Stratno | Stratigraphic Name | Reference Id | Usage No |   Usage  | Page Number | Minimum Age Name | Maximum Age Name | Reference Comments | Numerical Age | Parent Units | Constituents | Related Units | Lithology | Last Update
80891|Abbey Peak granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Saint Pauls Hill Suite.||||
37738|Accident Subgroup|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the South Nicholson Group.||||||
37738|Accident Subgroup|64443|6|Mentioned|p3-4|Calymmian|Calymmian|Of South Nicholson Group. Overlies Wild Cow Subgroup. Includes the Mittiebah Sandstone, Constance Sandstone and Mullera Formation.||||||
37738|Accident Subgroup|65336|5|Briefly described|Map Legend|Calymmian|Calymmian|Of South Nicholson Group. Includes Mittiebah Sandstone. Unconformably underlies Helen Springs Volcanics of Kalkarindji Volcanic Group.||||||
37738|Accident Subgroup|65337|3|Fully described|p v, pp50-60, p86.|Mesoproterozoic|Mesoproterozoic|400 - 3350 m thick. Sandstone-dominant basal part forms resistant ridges. Parent unit correlated with Roper Group, giving an approximate, interpreted, age. |c.1500-1400 Ma.|Unit in South Nicholson Group.|Includes Constance, Mittiebah and Tidna Sandstones and Mullera Formation.|Overlies Wild Cow Subgroup.|Fine-grained shelf tempestites and shales, and coarse-grained fluvial and shallow-marine siliciclastic rocks.|
37738|Accident Subgroup|67150|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||Unit in South Nicholson Group.|May include Mittiebah Sandstone.|||17-OCT-11
37738|Accident Subgroup|67352|5|Briefly described|p12-16|Calymmian|Calymmian|||South Nicholson Group|Mittiebah Sandstone|Overlies Wild Cow Subgroup||
37738|Accident Subgroup|68146|4|Described|p28, p196|||South Nicholson Basin. Fig.150 on p106 (by I. Sweet, in preparation) places the Constance Sandstone in the Wild Cow Subgroup, below an unconformity; above which the Elizabeth Sandstone Member is shown as basal Accident Subgroup but without a parent Formation.||South Nicholson Group.|Constance Sandstone, Tidna Sandstone, Mullera Formation, Elizabeth Sandstone Member. See Comments.|Unconformably overlies Wild Cow Subgroup.||
37738|Accident Subgroup|69434|4|Described|p19:2-3, 5-7|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. 400-3350m thick. The various Formations or Members interdigitate, or grade laterally and vertically into one another, over tens of kms of strike.||South Nicholson Group.|Mullera Formation, Constance and Mittiebah Sandstones; also Tidna Sandstone (in QLD).|Overlies Wild Cow Subgroup in the W and SW, conformably to unconformably. Overlies McNamara and Fickling Groups and Caulfield beds unconformably or disconformably.||12-JUL-16
37738|Accident Subgroup|69591|4|Described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). From ~1000m to ~3500m thick.||South Nicholson Group.|Elizabeth Sandstone, Mullera Formation, Tidna Sandstone.|Overlies Wild Cow Subgroup.||
37738|Accident Subgroup|69673|6|Mentioned|p56|||Minimum thickness of 400m in the NT.|||Includes Constance Sandstone, Mittiebah Sandstone, Mullera Formation|Disconformably overlies the Wild Cow Subgroup||
37738|Accident Subgroup|70968|5|Briefly described|p131 Fig.118, p132|Ectasian|Calymmian|||South Nicholson Group.|Mullera Formation; Mittiebah, Constance Sandstones.|Unconformably overlies Wild Cow Subgroup.||
37738|Accident Subgroup|71369|5|Briefly described|p1, p6, p8, p23, p36|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin.||South Nicholson Group.|Constance, Elizabeth, Tidna Sandstones; Mullera Formation.|Unconformably overlies Constance Sandstone (Wild Cow Subgroup).||
37738|Accident Subgroup|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstoen.|||
37738|Accident Subgroup|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstoen.|||
37738|Accident Subgroup|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstone.|||26-NOV-19
37738|Accident Subgroup|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstone.|||19-MAR-20
37738|Accident Subgroup|72418|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72421|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72422|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72423|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72526|4|Described|p8 Fig.1.3, p33-34, p56, p67, p86.|Mesoproterozoic|Mesoproterozoic|Shown as located in the South Nicholson Basin.||South Nicholson Group|Constance Sandstone, Mittiebah Sandstone, Mullera Formation.|Shown as unconformably overlying Benmara Group and Fickling Group.|Includes sandstone and green-grey claystone, siltstone, conglomerate.|
37738|Accident Subgroup|72527|4|Described|p3, p7 Fig.1.4, p41, p193, p195-196.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Rawlings et al., (2008) describe Burangoo Sandstone Member as a constituent of the Accident Subgroup.||South Nicholson Group|Includes Buddycurrawa Volcanics, Burangoo Sandstone Member and Constance Sandstone.|Unconformably overlies Wild Cow Subgroup and unconformably underlies Bukalara Sandstone.||
37738|Accident Subgroup|72912|4|Described|p5 Fig.3, p21, p23-24, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the West, Central and East parts of the South Nicholson Basin. In the Central part of the Basin, this unit forms the entire succession and is 2km thick in total.||South Nicholson Group|Mullera Formation,Train Range Ironstone, Mittiebah Sandstone and Constance Sandstone.|Overlies Wild Cow Subgroup.|Includes ironstone, siltstone, dolomitic siltstone, sandstone.|
37738|Accident Subgroup|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern part of the South Nicholson Basin.||South Nicholson Group|Mittebah Sandstone, Mullera Formation and Constance Sandstone|Overlies Wildcow Subgroup.|Includes sandstone, siltstone, dolomitic siltstone, ironstone,|
37738|Accident Subgroup|72919|6|Mentioned|p5, p47, p70, p77|Mesoproterozoic|Mesoproterozoic|Includes Constance Sandstone in NT but not in QLD.||South Nicholson Group|Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Mittiebah Sandstone, Constance Sandstone|Underlain by Crow Formation, including Tobacco Member (Wild Cow Subgroup). Unconformably overlain by Bukalara Sandstone.||
37738|Accident Subgroup|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||South Nicholson Group|Mullera Formation; Mittiebah, Constance sandstones; Middle Creek Sandstone, Train Range Ironstone and Bowthorn members.|Underlain by Crow Formation and Wallis Formation. Partly overlain by Tidna Sandstone.||
37738|Accident Subgroup|73144|6|Mentioned|p8, p13|Calymmian|Calymmian|South Nicholson Basin.||South Nicholson Group|Tidna Sandstone, Mullera Formation, Middle Creek Sandstone Member, Train Range Ironstone, Elizabeth Sandstone, Constance Sandstone, Schultz Sandstone Member, Bowthorn Member|Unconformably underlain by Wallis Formation (Wild Cow Subgroup).||
82282|Accommodation Creek Monzogranite|71628|4|Described|p12: 1, 3-4; p15: 40, 116|Early Triassic|Late Permian|New name. Previously included in Stanthorpe Monzogranite by Brown et al. (2007). Excluded from this author's definition of Stanthorpe Complex. Named after a local watercourse. Forms a thick (up to 350m wide), ~4 km long, NNW-trending dyke just N of Wallangarra. Limited geochemistry is briefly described.||Sailor Jack Suite.||Intrudes Wallangarra Volcanics.|Pale grey to pale brownish-grey, medium- to coarse-grained, highly porphyritic biotite-hornblende monzogranite. Has undergone deformation and alteration. I-type.|
75656|Adaluma Tonalite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, medium-grained, slightly porphyritic hornblende-biotite tonalite, biotite-hornblende granodiorite, and biotite quartz monzodiorite; foliated and partly recrystallised; with traces of allanite, titanite; attenuated mafic inclusions common.|
26290|Adler Hill Basalt|23497|5|Briefly described|Table 1|Pleistocene|Pliocene|Of Atherton Subprovince. of Willmott and others, 1988. Unconformable on Hodgkinson Formation rocks.||||||03-JUN-09
26290|Adler Hill Basalt|23506|5|Briefly described|Map Legend|Holocene|Miocene|||||||
26290|Adler Hill Basalt|23507|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
26290|Adler Hill Basalt|42625|5|Briefly described|Map legend|Pleistocene|Pliocene|Reserved.||||||
26290|Adler Hill Basalt|42810|2|Defined|Table 1 P14|Pleistocene|Pliocene|see also P29||||||
26290|Adler Hill Basalt|60425|6|Mentioned|p42 Tb. 3|Miocene|Miocene|Part of Atherton Basalt grouping.||||||07-FEB-11
27313|Agate Creek Volcanic Group|23032|6|Mentioned|p45|||||||||
27313|Agate Creek Volcanic Group|23220|5|Briefly described| p15|Permian|Carboniferous|Fossil assemblage includes rare plant fossils of early Permian age.||||||
27313|Agate Creek Volcanic Group|23291|4|Described|p43, p94 Tb.3.9|Early Permian|Early Permian|Originally mapped as Agate Creek Volcanics. Redefined by Oversby & Mackenzie (1995). Geological Province: Georgetown Region. Max. thickness: 400m.||||||08-JUL-15
27313|Agate Creek Volcanic Group|39917|6|Mentioned|Map legend|Permian|Permian|||||||
27313|Agate Creek Volcanic Group|40860|5|Briefly described|p115|||||||||
27313|Agate Creek Volcanic Group|43259|6|Mentioned|Appendix 1,p3.||Permian|||||||
27313|Agate Creek Volcanic Group|43664|6|Mentioned|p80|||||||||
27313|Agate Creek Volcanic Group|43740|4|Described|p30, 77|Permian|Permian|Max thickness 900m. Contains Early Permian flora Gangamopteris in the Black Soil Andesite.||||||01-SEP-04
27313|Agate Creek Volcanic Group|50199|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Thunder Egg Rhyolite, Black Soil Andesite, Talaveras Rhyolite, Big Surprise Tuff.||||||
27313|Agate Creek Volcanic Group|50210|5|Briefly described|Map Legend|Permian|Permian|Includes: Big Surprise Tuff.||||||
27313|Agate Creek Volcanic Group|50211|5|Briefly described|Map Legend|Early Permian|Early Permian|||||||
27313|Agate Creek Volcanic Group|68353|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||Includes Big Surprise Tuff; Talaveras and Thunder Egg Rhyolites; and Black Soil Andesite.|||
27313|Agate Creek Volcanic Group|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||Includes Big Surprise Tuff; Talaveras and Thunder Egg Rhyolites; and Black Soil Andesite.|||
27313|Agate Creek Volcanic Group|68415|5|Briefly described|Map Legend|Permian|Permian|Early Permian age. Of the Kennedy Province.|||Includes Big Surprise Tuff.||Includes grey, green, or brown basement-derived and locally volcanic lithic arenite to rudite; maar or diatreme fill.|
27313|Agate Creek Volcanic Group|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork, Mitchell River and Nychum Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
27313|Agate Creek Volcanic Group|69593|5|Briefly described|p490|Permian|Permian|Kidston Subprovince, Kennedy Igneous Association. Unassigned. Includes M-types, I-types and some A-types.|||||Slightly-moderately porphyritic basaltic andesite, andesite and basalt; also crystal-rich rhyolitic ignimbrite, rhyolite to dacite lava, and tuffaceous rocks; subordinate sediments.|
27313|Agate Creek Volcanic Group|72297|6|Mentioned|p755||||||Black Soil Andesite.|||
27313|Agate Creek Volcanic Group|72983|6|Mentioned|p70, p74, p76|early Permian|early Permian|Approximate age inferred from palaeontological data (Withnall et al., 1997). Includes an unnamed porphyritc, slightly flow-banded rhyolite sill from the Sherwood gold deposit.|||Zig Zag dyke|||
27685|Agate Downs Siltstone|23064|6|Mentioned|135|||Geological province: Mt Isa Inlier. Of Mary Kathleen Group.||||||15-MAR-07
27685|Agate Downs Siltstone|37862|4|Described|p588|||||||||
27685|Agate Downs Siltstone|38234|6|Mentioned|Fig.2|||||||||
27685|Agate Downs Siltstone|38235|6|Mentioned|p116|||||||||
27685|Agate Downs Siltstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27685|Agate Downs Siltstone|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
27685|Agate Downs Siltstone|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27685|Agate Downs Siltstone|39445|5|Briefly described|Table 2|||||||||
27685|Agate Downs Siltstone|39496|4|Described|p13|||||||||
27685|Agate Downs Siltstone|40840|6|Mentioned|Map legend|||||||||
27685|Agate Downs Siltstone|41306|4|Described|p12|||||||||
27685|Agate Downs Siltstone|41791|6|Mentioned|Fig.2|||||||||
27685|Agate Downs Siltstone|45161|4|Described|p50|||||||||
27685|Agate Downs Siltstone|45166|4|Described|p24|||||||||
27685|Agate Downs Siltstone|49009|1|Redefined|p2|Proterozoic|Proterozoic|Formerly Agate Downs Siltstone Member of the Staveley Formation||||||
27685|Agate Downs Siltstone|50100|5|Briefly described|p11, p20|Proterozoic|Proterozoic|Overlies the Staveley Formation conformably.  Cherty and slaty metasiltstone, phyllite quartzite and minor breccia.  Geological Province: Eastern Fold Belt Province.||||||20-MAR-18
27685|Agate Downs Siltstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Metasiltstone, phyllite, quartzite.||||||
27685|Agate Downs Siltstone|64250|5|Briefly described|p7-8, p14, p15, p20|||Omitted from stratigraphic chart because of limited exposure.|1675-1610|Young Australia Group||Overlies or is lateral equivalent of Marimo Slate.||
27685|Agate Downs Siltstone|65396|6|Mentioned|p16-17, p169, p178, p180, p183, p189-190|Statherian|Statherian|See also p202. The authors propose grouping this and other siliciclastic units of the Mary Kathleen Group into the informal Young Australia Group. Said to be likely a lateral facies equivalent of Marimo Slate. The diagram on p17, reproduced on p183, shows the Agate Downs Siltstone conformably overlying Marimo Slate aged 1655 +/- 4 Ma, at the same time unconformably underlying Marimo Slate aged <1610 +/- 5 Ma.|1675 - 1610 Ma|Young Australia Group||Overlies Marimo Slate; conformably overlies Staveley Formation.||
27685|Agate Downs Siltstone|67323|6|Mentioned|p18|||Obsolete name; these rocks are now included in the Answer Slate.||||||
27685|Agate Downs Siltstone|67539|6|Mentioned|p13|||Correlated with the upper Formation of the Kuridala Group. Reassigned along with the Marimo Slate and Answer Slate as the Answer Slate, Kuridala Group.||||||
27685|Agate Downs Siltstone|69591|6|Mentioned|p46|||Obsolete: now included within Answer Slate.||||||
27685|Agate Downs Siltstone|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain. Probably unconformably underlying Answer Slate.||||Probably unconformably underlies Answer Slate.|Pale green to grey siltstone; minor very fine -grained calcareous sandstone and breccia.|
27685|Agate Downs Siltstone|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain. Probably unconformably underlying Answer Slate.||||Probably unconformably underlies Answer Slate.|Pale green to grey siltstone; minor very fine -grained calcareous sandstone and breccia.|
27685|Agate Downs Siltstone|72889|6|Mentioned|p8.|||||||||
78905|Ah Fat Granodiorite Complex|65388|3|Fully described|p242-243, p236, 247-8, 250, 251,276,321|Late Carboniferous|Late Carboniferous|Southern Auburn Arch. Previously Ah Fat Granite Complex, and prior to that, included in Kilbeggan Adamellite. In contact with the Evandale Tonalite, Glisson Granodiorite and Dogherty Granite. Assigned similar age to Evandale Tonalite based on similar form. Probably intruded by Impey Granodiorite. It probably intrudes the Torsdale Volcanics to the west. Mainly pinkish grey to grey, medium to coarse-grained, equigranular to seriate or slightly porphyritic biotite granite and hornblende-biotite granite to granodiorite. Abbreviated as Ah Fat Complex Fig. 85.||||||
78905|Ah Fat Granodiorite Complex|68679|5|Briefly described|p406-408|Carboniferous|Carboniferous|See also Ah Fat Granite Complex (p404).||||Intrudes Torsdale Volcanics (probably). Is intruded by Sujeewong Gabbro (probably).|Felsic, mainly medium- to coarse-grained, equigranular to seriate to porphyritic hornblende-biotite and leucocratic biotite granite along with the dominant granodiorite.|
25756|Airlie Volcanics|30914|6|Mentioned|Map legend|Permian|Permian|||||||
25756|Airlie Volcanics|32553|4|Described|p44|||||||||
25756|Airlie Volcanics|32554|4|Described|Table 1|||||||||
25756|Airlie Volcanics|32555|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25756|Airlie Volcanics|34408|6|Mentioned|p185|||On Table||||||
25756|Airlie Volcanics|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25756|Airlie Volcanics|36906|6|Mentioned|p25|||||||||
25756|Airlie Volcanics|37675|6|Mentioned|p2|||||||||
25756|Airlie Volcanics|39252|5|Briefly described|p21|||||||||
25756|Airlie Volcanics|39445|5|Briefly described|Table 8|||||||||
25756|Airlie Volcanics|42281|5|Briefly described|p72|||||||||
25756|Airlie Volcanics|42547|5|Briefly described|p48|||Permian||||||
25756|Airlie Volcanics|45151|6|Mentioned|p15|||||||||
25756|Airlie Volcanics|48921|2|Defined|p22|Early Permian|Early Permian|See also Table 1||||||
25756|Airlie Volcanics|65706|4|Described|p11, p16 Tbl.1, p17 Tbl.1, p18 Tbl.1,|Triassic|Early Permian|Whitsunday Subprovince. Assigned to the Early Permian but suspected to be Triassic. Possibly equivalent to Carmila beds; probably unconformable on Edgecumbe beds.||||Faulted against Whitsunday Volcanics; unconformably underlies Proserpine Volcanics.|Acid to intermediate volcaniclastics and lavas.|
25756|Airlie Volcanics|68358|6|Mentioned|p7|||||||||
25756|Airlie Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Campwyn Subprovince. ||||||
25756|Airlie Volcanics|68679|6|Mentioned|p347, p364|Permian|Permian|Northern New England Orogen.||||||
25756|Airlie Volcanics|68901|6|Mentioned|p2 Fig. i|Permian|Permian|New England Orogen, Bowen region.||||||26-SEP-18
25756|Airlie Volcanics|69952|6|Mentioned|p85|Permian|Permian|New England Orogen.||||||
25756|Airlie Volcanics|73197|6|Mentioned|p476 Fig.7, p479|Middle Triassic|Guadalupian|New England Orogen, northern. Undated, possibly of a similar age to the adjacent Gloucester Granite (U-Pb 243 Ma).|265-240 Ma||||Volcanics.|
75120|Airport Suite|60425|5|Briefly described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Supersuite. Contains the Airport Quartz Diorite. I-type.||||||07-FEB-11
41264|Aisbetts Granodiorite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Sparsely porphyritic hornblende-biotite granodiorite.||||||
41264|Aisbetts Granodiorite|65388|3|Fully described|p300-301,  Fig 98, p340|Early Triassic|Late Permian|Of Tandora Suite. Previously mapped within undifferentiated Rawbelle batholith. Probably younger than Evandale Tonalite, intrudes and may have partly recrystallised the Horse Granite Gneiss.  Mainly grey, equigranular to slightly porphyritic, medium-grained hornblende-biotite granodiorite.||||||
41264|Aisbetts Granodiorite|68679|5|Briefly described|p418|||Southern part of the Rawbelle Batholith. Ovoid pluton, ~20 km2.||||Intrudes Horse Granite Gneiss, Tandora Suite.|Unfoliated hornblende-biotite granodiorite.|
33153|Aitken Creek Gabbro|60481|5|Briefly described|Map Legend|Late Permian|Late Permian|Medium to coarse grained biotite hornblende pyroxene gabbro.||||||16-APR-21
33153|Aitken Creek Gabbro|61035|5|Briefly described|p17 Tb. 2|Triassic|Permian|Intrudes Glenprairie beds and Rookwood Volcanics; locally affected by deformation associated with the Marlborough Thrust. Medium to coarse-grained biotite-hornblende-pyroxene gabbro.||||||07-FEB-11
33153|Aitken Creek Gabbro|65388|2|Defined|p429-430, 428|Late Permian|Late Permian|Intrudes Glenprairie beds. In contact with Copperville Granodiorite. K-Ar age range: 249+/-5Ma to 255+/-5Ma, possibly reset. Includes varieties of dark grey, medium to coarse-grained gabbro in type area.||||||03-SEP-14
33153|Aitken Creek Gabbro|68359|6|Mentioned|p8|Early Triassic|Late Permian|||||Intrudes Glenprairie beds.||05-MAR-19
33153|Aitken Creek Gabbro|68679|5|Briefly described|p308, p423, p426|||Yarrol belt. An arcuate 10 km2 unit, 12km N of Marlborough; possibly more extensive (~10 x 5 km) under cover. Magnetic data briefly discussed. Several other similar ages given.|252 +/- 5 Ma (Webb and McDougall, 1968).|||Intrudes Glenprairie beds.|Biotite-hornblende-pyroxene gabbro; possibly has a more felsic core.|
23324|Alabama Diorite|23062|6|Mentioned|260|||||||||
23324|Alabama Diorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 454. I-Type.||||||
23324|Alabama Diorite|41659|6|Mentioned|p363|||||||||
23324|Alabama Diorite|41668|3|Fully described|p33|||||||||
23324|Alabama Diorite|42054|6|Mentioned|p272|||||||||
23324|Alabama Diorite|43259|4|Described|Appendix 1,p48.|Devonian|Ordovician|Devonian?||||||
23324|Alabama Diorite|50552|5|Briefly described|p1048 Fig.2||Late Silurian|In Lolworth-Ravenswood Terrane.||||||
36381|Albany Pass beds|23425|5|Briefly described|p381.|||Also see Plate 9.2 Carpentaria Basin Province.||||||
36381|Albany Pass beds|23430|5|Briefly described|p522|||||||||
36381|Albany Pass beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
36381|Albany Pass beds|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
36381|Albany Pass beds|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||||||
36381|Albany Pass beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Helby beds under the symbol, JKh.||||||
36381|Albany Pass beds|69594|5|Briefly described|p520-521, p540-541|||Powell et al. (1976). Western Gulf Sub-basin (Cape York Peninsula), Carpentaria Basin; Peninsula Basin. Poorly understood. 12m thick. Probably fluvial deposits.||||Equivalent to the Helby beds. Part-equivalent to Dalrymple Sandstone (Laura Basin).|Sandstone.|
36381|Albany Pass beds|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Carpentaria Basin.||||Overlies Helby beds. Is overlain by Wallumbilla FZ.||
36381|Albany Pass beds|73083|6|Mentioned|p69|||||||||
28014|Alberts Creek Monzogranite|23420|5|Briefly described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite.||||||
28014|Alberts Creek Monzogranite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Sugarbag Creek Quartzite. Medium to dark grey equigranular biotite monzogranite.||||||15-JAN-09
28014|Alberts Creek Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
24652|Aldebaran Sandstone|13516|5|Briefly described|p145 fig 3, p146 fig 4, p147, p150-154|Late Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP32 - APP5002||||||
24652|Aldebaran Sandstone|22601|6|Mentioned|414|Permian|Permian|Geol province Bowen Basin||||||
24652|Aldebaran Sandstone|22975|5|Briefly described|p34 Fig.6|Late Permian|Early Permian|||||||
24652|Aldebaran Sandstone|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
24652|Aldebaran Sandstone|22978|6|Mentioned|p148 Fig.1|||||||||
24652|Aldebaran Sandstone|22980|5|Briefly described|p249 Fig.2|Late Permian|Early Permian|||||||
24652|Aldebaran Sandstone|22982|6|Mentioned|p267|||||||||
24652|Aldebaran Sandstone|23006|5|Briefly described|p447 Fig.2|Permian|Permian|||||||
24652|Aldebaran Sandstone|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
24652|Aldebaran Sandstone|24077|5|Briefly described|p410 Tb. 2|Early Permian|Early Permian|Of the Gebbie Subgroup.  Sandstone, feldspathic to orthoquartzitic, conglomeratic, massive conglomerate.  Max. thickness: 640m.  Geological Province: Bowen Basin.||||||
24652|Aldebaran Sandstone|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: >259Ma.  Geological Province: Bowen Basin.||||||
24652|Aldebaran Sandstone|24241|5|Briefly described|p18|Late Permian|Late Permian|Of Back Creek Group. Geological Province: Bowen Basin.||||||
24652|Aldebaran Sandstone|29391|6|Mentioned|Table 3|||See P18||||||
24652|Aldebaran Sandstone|29393|6|Mentioned|Table 2|||||||||
24652|Aldebaran Sandstone|29410|6|Mentioned|p274|||Permian geological map.||||||
24652|Aldebaran Sandstone|29412|5|Briefly described|p209|||In table, see also Fig.2.||||||
24652|Aldebaran Sandstone|29414|6|Mentioned|p260|||||||||
24652|Aldebaran Sandstone|29721|6|Mentioned|Table 65|||||||||
24652|Aldebaran Sandstone|30340|6|Mentioned|Table 3|||||||||
24652|Aldebaran Sandstone|30341|6|Mentioned|p136|||Lower Permian age||||||
24652|Aldebaran Sandstone|30448|6|Mentioned|p100|||||||||
24652|Aldebaran Sandstone|30508|6|Mentioned|p92|||Palynological subdivision||||||
24652|Aldebaran Sandstone|30545|6|Mentioned|Fig.2|||Lower Permian||||||
24652|Aldebaran Sandstone|30546|6|Mentioned|p107|||Permian age. Correlation||||||
24652|Aldebaran Sandstone|30743|6|Mentioned|p32|||Correlation. Late Artinskian age.||||||
24652|Aldebaran Sandstone|30826|6|Mentioned|p634|||||||||
24652|Aldebaran Sandstone|30914|6|Mentioned|Map legend|Permian|Permian|||||||
24652|Aldebaran Sandstone|31079|6|Mentioned|p5|||||||||
24652|Aldebaran Sandstone|31120|4|Described|p150|||||||||
24652|Aldebaran Sandstone|31305|6|Mentioned|p569|||||||||
24652|Aldebaran Sandstone|32139|6|Mentioned|p579|||||||||
24652|Aldebaran Sandstone|32577|4|Described|p23|||L.Perm. See also P24,27,33,36,42.||||||
24652|Aldebaran Sandstone|32834|6|Mentioned|Table 3|||||||||
24652|Aldebaran Sandstone|32837|6|Mentioned|p170|||Refers Paten (1969)||||||
24652|Aldebaran Sandstone|32840|6|Mentioned|p1,29|||Stratigraphy & biostratigraphy.||||||
24652|Aldebaran Sandstone|32945|6|Mentioned|p81|||Permian. See also Fig.3||||||
24652|Aldebaran Sandstone|33144|6|Mentioned|p67|||||||||
24652|Aldebaran Sandstone|33366|6|Mentioned|Fig.3|||Perm.||||||
24652|Aldebaran Sandstone|33701|6|Mentioned|Fig.1|||Artinskian.||||||
24652|Aldebaran Sandstone|33745|6|Mentioned|p204|||See also Figs 2 & 3||||||
24652|Aldebaran Sandstone|34132|6|Mentioned|p5|||Lower Permian. See also P2.||||||
24652|Aldebaran Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
24652|Aldebaran Sandstone|34390|4|Described|Table 2|||Permian||||||
24652|Aldebaran Sandstone|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
24652|Aldebaran Sandstone|34415|6|Mentioned|p82|||||||||
24652|Aldebaran Sandstone|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
24652|Aldebaran Sandstone|35079|6|Mentioned|p424|||||||||
24652|Aldebaran Sandstone|35148|6|Mentioned|p411|||||||||
24652|Aldebaran Sandstone|35150|6|Mentioned|p420|||||||||
24652|Aldebaran Sandstone|35238|6|Mentioned|Fig.4|||||||||
24652|Aldebaran Sandstone|35284|6|Mentioned|Fig.1|||||||||
24652|Aldebaran Sandstone|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
24652|Aldebaran Sandstone|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin. Lithology described P184.||||||
24652|Aldebaran Sandstone|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
24652|Aldebaran Sandstone|35554|6|Mentioned|Fig.1|||||||||
24652|Aldebaran Sandstone|35811|5|Briefly described|Table 5|||||||||
24652|Aldebaran Sandstone|35873|6|Mentioned|p56|||||||||
24652|Aldebaran Sandstone|35901|6|Mentioned|p5|||||||||
24652|Aldebaran Sandstone|35937|6|Mentioned|p619|||||||||
24652|Aldebaran Sandstone|36103|4|Described|Table 1|||||||||
24652|Aldebaran Sandstone|36104|6|Mentioned|p122|||||||||
24652|Aldebaran Sandstone|36233|6|Mentioned|p152|||||||||
24652|Aldebaran Sandstone|36241|4|Described|p115|||||||||
24652|Aldebaran Sandstone|36243|6|Mentioned|Table 3A|||||||||
24652|Aldebaran Sandstone|36739|6|Mentioned|Fig.2|||||||||
24652|Aldebaran Sandstone|36899|6|Mentioned|p1091|||||||||
24652|Aldebaran Sandstone|37070|4|Described|p72|||||||||
24652|Aldebaran Sandstone|37072|4|Described|p90|||||||||
24652|Aldebaran Sandstone|37133|6|Mentioned|p377|||||||||
24652|Aldebaran Sandstone|37139|6|Mentioned|p78|||||||||
24652|Aldebaran Sandstone|37610|6|Mentioned|Fig.4|||||||||
24652|Aldebaran Sandstone|37612|3|Fully described|p289|||See also P283 and Fig.3.||||||
24652|Aldebaran Sandstone|37705|6|Mentioned|Fig.2|||||||||
24652|Aldebaran Sandstone|37724|6|Mentioned|Table 1|||||||||
24652|Aldebaran Sandstone|37726|3|Fully described|p145|||||||||
24652|Aldebaran Sandstone|37858|6|Mentioned|p85|||||||||
24652|Aldebaran Sandstone|37918|6|Mentioned|p474|||||||||
24652|Aldebaran Sandstone|38092|6|Mentioned|p284|||||||||
24652|Aldebaran Sandstone|38198|6|Mentioned|p414|||||||||
24652|Aldebaran Sandstone|38204|6|Mentioned|p79|||||||||
24652|Aldebaran Sandstone|38312|4|Described|p460|||||||||
24652|Aldebaran Sandstone|38518|6|Mentioned|Fig.3|||||||||
24652|Aldebaran Sandstone|38917|6|Mentioned|p170|||||||||
24652|Aldebaran Sandstone|38955|4|Described|p313|||||||||
24652|Aldebaran Sandstone|39212|5|Briefly described|p11|||P24-gas reservoir. See also P33||||||
24652|Aldebaran Sandstone|39252|6|Mentioned|Fig.13|||||||||
24652|Aldebaran Sandstone|39253|6|Mentioned|p34|||in SQD 1(Morella). See also P36||||||
24652|Aldebaran Sandstone|39261|6|Mentioned|Fig.6|||||||||
24652|Aldebaran Sandstone|39263|6|Mentioned|Fig.1|||||||||
24652|Aldebaran Sandstone|39264|6|Mentioned|Fig. 4|||||||||
24652|Aldebaran Sandstone|39267|6|Mentioned|p236|||||||||
24652|Aldebaran Sandstone|39272|6|Mentioned|Fig. 3|||||||||
24652|Aldebaran Sandstone|39273|4|Described|p305|||||||||
24652|Aldebaran Sandstone|39275|6|Mentioned|Fig. 11|||||||||
24652|Aldebaran Sandstone|39412|6|Mentioned|p13|||||||||
24652|Aldebaran Sandstone|39423|6|Mentioned|p47|||||||||
24652|Aldebaran Sandstone|39445|5|Briefly described|Table 8|||||||||
24652|Aldebaran Sandstone|39494|6|Mentioned|p129|||See also Fig.5||||||
24652|Aldebaran Sandstone|39611|6|Mentioned|Fig.2|||||||||
24652|Aldebaran Sandstone|39757|6|Mentioned|p1601|||||||||
24652|Aldebaran Sandstone|39813|6|Mentioned|Map legend|Permian|Carboniferous|Permo Carboniferous||||||
24652|Aldebaran Sandstone|39815|6|Mentioned|Fig.10|||||||||
24652|Aldebaran Sandstone|39943|6|Mentioned|Table 5A|||||||||
24652|Aldebaran Sandstone|39994|6|Mentioned|p200|||||||||
24652|Aldebaran Sandstone|39999|6|Mentioned|p246|||||||||
24652|Aldebaran Sandstone|40030|6|Mentioned|p135|||||||||
24652|Aldebaran Sandstone|40539|6|Mentioned|Fig.2|||||||||
24652|Aldebaran Sandstone|40544|6|Mentioned|Fig.6|||||||||
24652|Aldebaran Sandstone|40623|5|Briefly described|p110|||||||||
24652|Aldebaran Sandstone|41173|6|Mentioned|Table 2|||||||||
24652|Aldebaran Sandstone|41191|6|Mentioned|Fig.3|||||||||
24652|Aldebaran Sandstone|41246|6|Mentioned|Map legend|Permian||||||||
24652|Aldebaran Sandstone|41247|6|Mentioned|p128|||See also Fig.7||||||
24652|Aldebaran Sandstone|41275|6|Mentioned|p30|||||||||
24652|Aldebaran Sandstone|41290|6|Mentioned|Fig.8|||||||||
24652|Aldebaran Sandstone|41330|6|Mentioned|Table 1|||||||||
24652|Aldebaran Sandstone|41605|6|Mentioned|Fig.2|||||||||
24652|Aldebaran Sandstone|41666|6|Mentioned|p26|||||||||
24652|Aldebaran Sandstone|41689|6|Mentioned|Table 1|||||||||
24652|Aldebaran Sandstone|41725|6|Mentioned|p404|||||||||
24652|Aldebaran Sandstone|41737|6|Mentioned|p351|||||||||
24652|Aldebaran Sandstone|41809|6|Mentioned|p65|||||||||
24652|Aldebaran Sandstone|42187|6|Mentioned|p318|||||||||
24652|Aldebaran Sandstone|42212|6|Mentioned|p329|||||||||
24652|Aldebaran Sandstone|42249|6|Mentioned|p21|||||||||
24652|Aldebaran Sandstone|42250|6|Mentioned|p31|||||||||
24652|Aldebaran Sandstone|42252|6|Mentioned|Fig.1 P47|||||||||
24652|Aldebaran Sandstone|42253|5|Briefly described|Fig.2 P217|||||||||
24652|Aldebaran Sandstone|42254|6|Mentioned|p221|||||||||
24652|Aldebaran Sandstone|42309|6|Mentioned|p289|||||||||
24652|Aldebaran Sandstone|42437|3|Fully described|p820||Early Permian|||||||
24652|Aldebaran Sandstone|42578|5|Briefly described|Table 1 P124-125|||Name assumed. Actually spelt Aldebaran Ss.||||||
24652|Aldebaran Sandstone|42614|5|Briefly described|p13|||Bowen Basin||||||
24652|Aldebaran Sandstone|42621|4|Described|p273|||Lower Permion||||||
24652|Aldebaran Sandstone|42641|6|Mentioned|Fig.3 P110|||||||||
24652|Aldebaran Sandstone|42648|6|Mentioned|Fig.6 P41|||||||||
24652|Aldebaran Sandstone|42662|6|Mentioned|p84 Fig.4|||||||||
24652|Aldebaran Sandstone|42808|4|Described|p156|||see also Fig.1 P157||||||
24652|Aldebaran Sandstone|42856|5|Briefly described|Fig.2 P632|||||||||
24652|Aldebaran Sandstone|42865|5|Briefly described|p18|||||||||
24652|Aldebaran Sandstone|42911|6|Mentioned|p8|||||||||
24652|Aldebaran Sandstone|42974|6|Mentioned|p197|||||||||
24652|Aldebaran Sandstone|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
24652|Aldebaran Sandstone|43017|5|Briefly described|Fig.3,p375|||||||||
24652|Aldebaran Sandstone|43018|6|Mentioned|p392|||||||||
24652|Aldebaran Sandstone|43029|5|Briefly described|p23|||||||||
24652|Aldebaran Sandstone|43050|5|Briefly described|Fig.1,p5|||||||||
24652|Aldebaran Sandstone|43099|5|Briefly described|p10|||||||||
24652|Aldebaran Sandstone|43185|5|Briefly described|6-8||Late Permian|||||||
24652|Aldebaran Sandstone|43204|5|Briefly described|Map Legend|Late Permian|Early Permian|Denison Trough||||overlies Reids Dome beds and Cattle Creek Formation||23-DEC-11
24652|Aldebaran Sandstone|43213|5|Briefly described|p10, p55, p152-154, p239|Permian|Permian|Subdivided by Mollan et al. (1969) into three informal members. Power (1966) considered the top member to be a separate unit, the Freitag Formation.||||Overlies Reids Dome beds.|Feldspathic to quartzose sandstone interbedded with carbonaceous shale and fine coal seams; overlain by cross-bedded, pebbly, quartzose sandstone and conglomerate; then thinly interbedded sandstone, siltstone and mudstone with minor coal seams.|
24652|Aldebaran Sandstone|43580|6|Mentioned|Fig.1,p360|||||||||
24652|Aldebaran Sandstone|43714|5|Briefly described|p8|||||||||
24652|Aldebaran Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
24652|Aldebaran Sandstone|43883|14|Not recorded|p18 Fig.4-3||Permian|||||||
24652|Aldebaran Sandstone|43977|14|Not recorded|p576|||See also Lexicon.||||||
24652|Aldebaran Sandstone|43987|14|Not recorded|p267,270,281|||||||||
24652|Aldebaran Sandstone|43990|14|Not recorded|Map Legend|||Part of Gebbie Sub-Group.||||||
24652|Aldebaran Sandstone|43994|14|Not recorded|Map Legend|||||||||
24652|Aldebaran Sandstone|43995|14|Not recorded|Tb p9,17-8,53,fig.14||Permian|=Serocold Sandstone.||||||
24652|Aldebaran Sandstone|44022|14|Not recorded|Map Legend||Early Permian|||||||
24652|Aldebaran Sandstone|44023|4|Described|Tb.2,p6||Early Permian|||||||
24652|Aldebaran Sandstone|44040|14|Not recorded|p18|||||||||
24652|Aldebaran Sandstone|44079|14|Not recorded|p51|||||||||
24652|Aldebaran Sandstone|44081|14|Not recorded|Plate 9|||||||||
24652|Aldebaran Sandstone|44085|2|Defined|p4,9,10,15|||||||||
24652|Aldebaran Sandstone|44091|14|Not recorded|p45|||Part of Middle Bowen Group in Springsure area.||||||
24652|Aldebaran Sandstone|44096|14|Not recorded|p190-193|||=Serocold Sandstone||||||
24652|Aldebaran Sandstone|44169|2|Defined|Tb.1,p4,6,7,12,13|||||||||
24652|Aldebaran Sandstone|44170|4|Described|p6,10,11,29,30,33|||||||||
24652|Aldebaran Sandstone|44172|2|Defined|p1320,1323,Fig.2,||Artinskian|Tb.1,p1327-8,1330-3,1337,1342-3||||||
24652|Aldebaran Sandstone|44173|14|Not recorded|p109-113||Early Permian|||||||
24652|Aldebaran Sandstone|44218|14|Not recorded|p19||Kungurian|Early Kungurian.||||||
24652|Aldebaran Sandstone|44219|14|Not recorded|Fig.3,p9||Permian|||||||
24652|Aldebaran Sandstone|44243|4|Described|p645,647||Permian|Coal seams.||||||
24652|Aldebaran Sandstone|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
24652|Aldebaran Sandstone|44419|14|Not recorded|p273,275|||No data.||||||
24652|Aldebaran Sandstone|44421|14|Not recorded|p8,9||Permian|||||||
24652|Aldebaran Sandstone|44422|14|Not recorded|p150,152,153||Early Permian|||||||
24652|Aldebaran Sandstone|44571|14|Not recorded|p212|||||||||
24652|Aldebaran Sandstone|44604|14|Not recorded|p116,Fig.2,Tb.1|||||||||
24652|Aldebaran Sandstone|44618|14|Not recorded|p517||Early Permian|||||||
24652|Aldebaran Sandstone|44630|14|Not recorded|p493|||||||||
24652|Aldebaran Sandstone|44651|14|Not recorded|p117,123,124|||||||||
24652|Aldebaran Sandstone|44855|14|Not recorded|p27|||||||||
24652|Aldebaran Sandstone|45006|14|Not recorded|Tb.1|||||||||
24652|Aldebaran Sandstone|45031|14|Not recorded|p9,Fig.3||Early Permian|||||||
24652|Aldebaran Sandstone|45071|3|Fully described|Table 6|||||||||
24652|Aldebaran Sandstone|45168|6|Mentioned|p6|||||||||
24652|Aldebaran Sandstone|46849|6|Mentioned|p192|||||||||
24652|Aldebaran Sandstone|46949|6|Mentioned|p105|||||||||
24652|Aldebaran Sandstone|46989|5|Briefly described|Table 1|||||||||
24652|Aldebaran Sandstone|48626|4|Described|p1,3,22,24,34-47,50,||Permian|p52-56,59,94-102,Fig1,2,Pl.1.||||||
24652|Aldebaran Sandstone|48630|14|Not recorded|p1,4-8,13,17-19,22-3|||Pls.1,2.||||||
24652|Aldebaran Sandstone|48845|14|Not recorded|p37,38|||||||||
24652|Aldebaran Sandstone|48847|14|Not recorded|p1,10,Pl.2|||||||||
24652|Aldebaran Sandstone|48898|6|Mentioned|Fig.4|||L.Permian. Gebbie Subgroup||||||
24652|Aldebaran Sandstone|48900|2|Defined|p33|Early Permian|Early Permian|||||||
24652|Aldebaran Sandstone|48919|5|Briefly described|Table 2|||L.Permian||||||
24652|Aldebaran Sandstone|48920|6|Mentioned|p87|||Palynology||||||
24652|Aldebaran Sandstone|48924|6|Mentioned|p10||Permian|Permian||||||
24652|Aldebaran Sandstone|48995|6|Mentioned|Fig.3|||||||||
24652|Aldebaran Sandstone|49644|5|Briefly described|Table|||||||||
24652|Aldebaran Sandstone|60286|6|Mentioned|p296 Fig.10|||||||||
24652|Aldebaran Sandstone|60369|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes Kettle Conglomerate Member. Overlies Cattle Creek Formation and Reids Dome Beds. Pebbly quartz sandstone, conglomerate, minor shale, siltstone, coal.||||||02-SEP-04
24652|Aldebaran Sandstone|61377|6|Mentioned|p156 Tb. SU2|Early Permian|Early Permian|A reservoir unit in Queensland.||||||07-FEB-11
24652|Aldebaran Sandstone|61609|6|Mentioned|p240|Permian|Permian|Geological Province: Denison Trough.||||||07-FEB-11
24652|Aldebaran Sandstone|61612|6|Mentioned|p271, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Denison Trough.||||||17-MAR-09
24652|Aldebaran Sandstone|61772|6|Mentioned|p130||Early Permian|||||||
24652|Aldebaran Sandstone|62357|5|Briefly described|p527|Middle Permian|Middle Permian|Geological Province: Bowen Basin (Denison Trough). ||||||
24652|Aldebaran Sandstone|63713|5|Briefly described|p1507 Fig.2, p1508, p1522-1523, p1530|Roadian|Kungurian|Denison Trough, Bowen Basin.||||Overlies Cattle Creek Formation. Is overlain by Ingelara and Freitag Formations.||
24652|Aldebaran Sandstone|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Early Permian|Bowen Basin.||||Overlies Cattle Creek Formation. Is overlain by Ingelara Formation.||
24652|Aldebaran Sandstone|64856|6|Mentioned|p49-51|||Denison Trough. Basal part correlated with Buffel Formation.| | ||||28-NOV-17
24652|Aldebaran Sandstone|64857|5|Briefly described|p114,116, p113 Fig.3|Early Permian|Early Permian|Bowen Basin. Overlies Cattle Creek Formation. Age: late Early Permian.||||||
24652|Aldebaran Sandstone|65113|6|Mentioned|p345|Late Permian|Early Permian|intra-Aldebaran Sandstone unconformity ~267Ma. See also informal upper Aldebaran Sandstone and lower Aldebaran Sandstone, used elsewhere in this paper.||||||
24652|Aldebaran Sandstone|65115|5|Briefly described|p413|||Includes a marked angular unconformity in the Denison Trough, mapped as the base of Supersequence C. On many seismic lines the unconformity is very subtle.||||||18-MAR-13
24652|Aldebaran Sandstone|65116|5|Briefly described|p442, p444, Fig 2 p436|Late Permian|Early Permian|Shown as upper and lower Aldebaran Sandstone, with time break over Palynological zones APP4.1-APP4.2 between. Overlies the Cattle Creek Formation and underlies the Freitag Formation in the Denison Trough, Bowen Basin||||||
24652|Aldebaran Sandstone|65118|5|Briefly described|p491, Fig 2 p479|Permian|Permian|Underlies the Freitag Formation, Denison Trough, Bowen Basin. Overlies the Cattle Creek Formation. Shown as upper Aldebaran and lower Aldebaran Sandstones.There is an unconformity within this unit.||||||06-MAR-12
24652|Aldebaran Sandstone|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p7, p8|||Denison Trough, Bowen Basin.||||||
24652|Aldebaran Sandstone|67402|4|Described|p64, p64 fig BWW2, p65, p66 fig BWW4|Wordian|Kungurian|See also, Aldebaran Sandstone, Lower and Upper. Deposited in tide to wave dominated delta, coastal and delta fan depositional environments. Seperated into two parts on the basis of an unconformity. See also p68, p69, p70, p72, p73, p75, p76, p79, p82, p84, p85 tbl BWN2, p302, p303.||||Overlies the Cattle Creek Formation. Overlain by the Freitag Formation.|Quartzose sandstone, conglomerate, shale, coal and lesser siltstone.|
24652|Aldebaran Sandstone|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by German Creek Formation or Freitag Formation.||
24652|Aldebaran Sandstone|68004|6|Mentioned|p173.|||Bowen Basin. Has hydrocarbon reservoir potential.||||||
24652|Aldebaran Sandstone|68576|5|Briefly described|Q_4: p3, p9|Lopingian|Cisuralian|Bowen Basin.||||Overlies Sirius Mudstone Member (Cattle Creek Formation). Is overlain by Freitag Formation.||
24652|Aldebaran Sandstone|68679|5|Briefly described|p378-381, p384|||Mollan et al. (1969). Bowen Basin. 650m thick. Delta sediments. A regional unconformity separates the lower and upper parts, marking a major change in Australia's tectonic setting. Produces gas and minor condensate.||||Gradationally overlies Cattle Creek Formation. Is overlain by Freitag Formation.|Quartzose sandstone, pebbly sandstone, conglomerate, siltstone, mudstone, minor coal.|
24652|Aldebaran Sandstone|68731|6|Mentioned|p201 Fig 3.110|Permian|Permian|Bowen Basin.||||||
24652|Aldebaran Sandstone|69599|5|Briefly described|p593|Permian|Permian||||Kettle Conglomerate Member.|||
24652|Aldebaran Sandstone|70856|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group.||Overlies Cattle Creek Formation.|Pebbly quartz sandstone, conglomerate, minor shale, siltstone and coal.|
24652|Aldebaran Sandstone|71265|5|Briefly described|p589-590, p595|Wuchiapingian|Roadian|Bowen and eastern Galilee Basins.||||Overlies Sirius Mudstone Member (Cattle Creek Formation). Is overlain by Freitag Formation.||
24652|Aldebaran Sandstone|71276|5|Briefly described|p287-288, p294, p295 Fig.8, p296-297|Lopingian|Lopingian|Eastern side of the Springsure Shelf (Denison Trough, Bowen Basin). Probable lateral equivalent of (part of) the Colinlea Sandstone.||||Is overlain by Freitag Formation.|Blocky sandstone.|
24652|Aldebaran Sandstone|71710|5|Briefly described|p380|||Geological province: Bowen Basin. Shows a disconformity within the formation, likely associated with uplift event in the New England Orogen||||Correlative to the Colinlea Sandstone in the southern Galilee Basin.||22-MAY-19
24652|Aldebaran Sandstone|72088|5|Briefly described|p8, p20, p38, p91|Wuchiapingian|Kungurian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Overlian by the Freitag Formation.||
24652|Aldebaran Sandstone|72297|5|Briefly described|p695, p724-725|||Bowen Basin. Contains sodium bicarbonate (25,000 mg/L at Warrinilla); source of the bicarbonate in brines in the Precipice Sandstone at Grafton Range, NE of Roma. Potential oil source rock.|||||Contains coal in thin seams and below coking rank.|
24652|Aldebaran Sandstone|73304|6|Mentioned|p78|||Bowen Basin, southern.||||||
24652|Aldebaran Sandstone|73472|6|Mentioned|p115|Wuchiapingian|Kungurian|Galilee Basin.||||Underlain by Sirius Mudstone Member (Cattle Creek Formation). Overlain by Freitag Formation. Equivalent to Colinlea Sandstone.||
39010|Alice Creek beds|23799|3|Fully described|p25, p15 Tb. 1|Early Carboniferous|Late Devonian|Originally considered to be part of  Permian Cressbrook Creek Group - fossil evidence later confirmed Late Devonian-Early Carboniferous age. Overlain by Woogaroo Subgroup.  Intruded by Mount Cross Igneous Complex.  Geological Province: Yarrol Province.||||||
39010|Alice Creek beds|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
39010|Alice Creek beds|24560|5|Briefly described|Map legend|Carboniferous|Devonian|Poorly fossiliferous limestone.||||||
39010|Alice Creek beds|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit is mapped with Mount Barney beds under the symbol, Cy.||||||
39010|Alice Creek beds|68679|4|Described|p306, p321, p351|Mississippian|Early Devonian|Exposed within a small (~2 km2) area along Alice Creek N of Helidon. Previously considered part of Cressbrook Creek Group until discovery of Leptophloem australe plant fossils. Continental margin forearc rocks. Considered an inlier of the Yarrol Province.||||Is intruded by, and faulted against, the Mount Cross Igneous Complex.|Limestone (possibly allochthonous), volcanilithic conglomerate (with pebbles of andesitic to rhyolitic fragments with minor chert in a feldspathic sandy matrix), and sandstone; minor interbedded chert, silicified siltstone and mudstone.|
83363|Alice Queen dyke|72983|5|Briefly described|p7, p41-42, p44-45|||[informal unit name]. Kennedy Igneous Association. Cape York region. Alice River Goldfield. Sampled dyke intrudes the Imooya Granite and may be related to gold mineralisation. Sample collected for SHRIMP U-Pb dating did not yield a statistically robust result; however, a single grain age of 279.9 +/- 5.8 Ma (2sig) may represent the magmatic crystallisation age.||||Intrudes the Imooya Granite.|Strongly sericitised, fine-grained sparsely porphiritic rhyolite.|
75628|Alick Creek Tonalite|70673|5|Briefly described|p5-10, p125-129|Early Cretaceous|Early Cretaceous|A small (c.3.5 km2) pluton, adjacent to Thurderbolt Granite. Part of a major magmatic event: within uncertainty of the Hecate Granite and Blackwall Quartz Diorite. Forms massive undeformed outcrops. Said to have the informal name of "Mother Gall granite".|134.0 +/- 0.8 Ma (SHRIMP).||||Leucocratic, pinkish-grey, fine- to medium-grained, slightly porphyritic biotite tonalite.|
75628|Alick Creek Tonalite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|134+/-0.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
69595|Allandale Granite|61155|5|Briefly described|p19|Late Oligocene|Early Oligocene|Overlain by Numinbah Valley Formation. Age:32-26Ma. In the Brisbane region.||||||
69595|Allandale Granite|63187|5|Briefly described|p106|Cenozoic|Cenozoic|Part of a silicic suite of the Noosa area volcanic units - comprising hypabyssal silicic rocks and minor mafic lavas.||||||19-NOV-08
69595|Allandale Granite|69599|5|Briefly described|p637|||Noosa hinterland. Mineralogy described.|||||Alkaline granite.|
69595|Allandale Granite|73450|4|Described|p84, p86|Chattian|Rupelian|Forms a small stock in the Noosa hinterland. Metaluminous but close to peralkaline. Its relationship (if any) with the Lakes View Granodiorite/syenite is unknown. Yielded a mineral Ar-Ar age of 27.6 +/- 0.4 Ma (Cohen et al., 2007). Also previously dated using K-Ar methods.|27.6 +/- 0.4 Ma Ar-Ar|||Intrudes Kin Kin beds and Myrtle Creek Sandstone.|Iron stained, leucocratic, medium grained phaneritic monzonite.|
69493|Allensleigh Basalt|69599|5|Briefly described|p594|Pliocene|Pliocene|Nulla Province.|3.6 Ma (Mackness et al., 2000).|||Overlies the Allingham Formation.||19-JUN-20
69493|Allensleigh Basalt|73115|6|Mentioned|p: 76-77, 90, 94, 99, 105, 110, 115, 120|Pliocene|Pliocene|Nulla Basalt Province. Interbedded with Campapse [Campaspe] Formation.|4.5-4.0 Ma|||||
29337|Almaden Granodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Almaden Supersuite.||||||24-JUL-08
29337|Almaden Granodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 303+/-5 Ma, Rb-Sr. Of the Almaden Supersuite.||||||29-APR-08
29337|Almaden Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 315. I-Type.||||||
29337|Almaden Granodiorite|23616|5|Briefly described|p41||Carboniferous|||||||
29337|Almaden Granodiorite|43060|5|Briefly described|p61|||Of Almaden Supersuite.||||||29-APR-08
29337|Almaden Granodiorite|43083|4|Described|p252|||Of Almaden Supersuite. I-type.  Intrudes Jamtin Rhyolite and Chillagoe and Hodgkinson Formations; cut by Hiker Granodiorite and Retchford, Jacks, Lucy, Burke and Billycan Granites. Lithology included.||||||17-JUN-09
29337|Almaden Granodiorite|43087|2|Defined|p48|Late Carboniferous||[Have assumed this name supersedes Almaden Granite]. Rb-Sr ages 301-302 Ma||||||17-AUG-15
29337|Almaden Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).  Hornblende-biotite granodiorite; biotite tonalite; hornblende-biotite granite.  Age: 302+/-5Ma.||||||29-APR-08
29337|Almaden Granodiorite|43259|4|Described|Appendix 1,p38.||Late Carboniferous|Age is 302+/-5 Ma.||||||
29337|Almaden Granodiorite|43626|6|Mentioned|p10||Late Carboniferous|||||||
29337|Almaden Granodiorite|60425|4|Described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Age: ~302-301Ma, 303+/-5Ma (Rb-Sr). I-type. Fine to medium-grained, variably porphyritic hornblend-biotite granodiorite and biotite-hornblende granodiorite. Significantly more lithological detail included.||||||07-FEB-11
29337|Almaden Granodiorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The three variants are mapped separately. Low K, Th and U radiometric responses.||Unit in Almaden Supersuite.|||Medium/dark grey, highly porphyritic biotite tonalite; medium/dark grey variably porphyritic granodiorite, mafic enclaves common, locally moderately to extensively altered; medium-grey to pink variably porphyritic hornblende-biotite monzogranite.|
29337|Almaden Granodiorite|69593|5|Briefly described|p510|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|305 Ma.|Almaden Supersuite.||||
30425|Almaden Suite|23624|5|Briefly described|p26|||||||||
30425|Almaden Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite (Almaden Supersuite).||||||15-JUN-06
30425|Almaden Suite|60425|5|Briefly described|p280-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite. Contains 12 named granites and Prices Dam Igneous Complex. I-type.||||||07-FEB-11
30425|Almaden Suite|69593|5|Briefly described|p484|||Western Hodgkinson Province.||Almaden Supersuite.|Almaden Granodiorite.||I-type.|
75358|Alpha Centauri Metamorphics|67323|5|Briefly described|p12, p31, p107, GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; . Post-Barramundi basement. Sybella Domain, Mount Isa Inlier. These rocks previously mapped as Eastern Creek Volcanics. |~1790 Ma protoliths.||||Layered calc-silicate rocks, fine-grained amphibolite and quartzite.|
75358|Alpha Centauri Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, as well as Bucket Hole Metavolcanics, Oroopo Metabasalt and Kallala Quartzite, are all mapped under the symbol, -Pvo.||||||25-JUL-13
75358|Alpha Centauri Metamorphics|69591|5|Briefly described|p29-30, p32, p41-42, p58|Paleoproterozoic|Paleoproterozoic|GSQ (2011). Sybella Domain, Mount Isa Province.|1789+/-4 Ma (MDA: Geoscience Australia unpub.data)|||Surrounds (is intruded by) the Sybella Granite.|Pelitic schist, amphibolite, calc-silicate, migmatised cordierite K-feldspar gneiss, sillimanite-biotite-K-feldspar gneiss and quartzite.|
27316|Altanmoui Granite|23423|5|Briefly described|p310 table 7.4||Early Permian|I-type granite. Part of the Cape Melville Supersuite.||||||24-JUL-08
27316|Altanmoui Granite|23430|5|Briefly described|p490|||||||||
27316|Altanmoui Granite|23512|5|Briefly described|Map Legend||Early Permian|||||||
27316|Altanmoui Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27316|Altanmoui Granite|37614|6|Mentioned|p240|||||||||
27316|Altanmoui Granite|39445|5|Briefly described|Table 12|||||||||
27316|Altanmoui Granite|42490|5|Briefly described|p15|||||||||
27316|Altanmoui Granite|43111|1|Redefined|p31||Early Permian|Rb-Sr rock-biotite age of about 277 Ma.||||||
27316|Altanmoui Granite|43896|14|Not recorded|Map Legend||Permian|||||||
27316|Altanmoui Granite|44267|14|Not recorded|Map Legend||Permian|||||||
27316|Altanmoui Granite|44292|2|Defined|Tb.1,opp.p8,p7-9||Permian|Porphyritic (muscovite) biotite adamellite.||||||
27316|Altanmoui Granite|45025|14|Not recorded|p79||Permian|||||||
27316|Altanmoui Granite|45113|3|Fully described|p23|||Emphasis on petrography.||||||
27316|Altanmoui Granite|60425|4|Described|p54 Tb. 4, p272-3 Appdx. 1|Early Permian|Early Permian|Of Cape Melville Supersuite. Intruded Hodgkinson Formation. I-type. Age: 277Ma (est.) (Rb-Sr). Medium-grained, mod'ly porphyritic biotite granite; accessory zircon, apatite, allanite; with scattered enclaves, biotite-rich schlieren and pegmatitic patches||||||07-FEB-11
27316|Altanmoui Granite|69593|5|Briefly described|p480, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|277 Ma.|Altanmoui Suite.|||I-type.|
69230|Altanmoui Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Cape Melville Supersuite. Contains Altanmoui Granite. I-type. Parts have been subsequently mapped as granite of the Wakooka Supersuite.||||||07-FEB-11
69230|Altanmoui Suite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |||Altanmoui Granite.|||
40103|Alton Downs Basalt|24615|5|Briefly described|CD|Late Cretaceous|Late Cretaceous|[Kva].  Olivine- and feldspar-phyric basalt.||||||
40103|Alton Downs Basalt|50209|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
40103|Alton Downs Basalt|50212|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
40103|Alton Downs Basalt|50317|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Olivine and feldspar-phyric basalt.||||||09-JUN-04
40103|Alton Downs Basalt|60557|5|Briefly described|p18 Fig. 5a, p28|Late Cretaceous|Late Cretaceous|Age: 67.3+/-2.6Ma (Wellman 1978).  See also p19 Fig. 5b.||||||09-JUN-05
40103|Alton Downs Basalt|65388|6|Mentioned|p50|Cretaceous|Cretaceous|Unconformably overlies Youlambie Conglomerate.||||||
40103|Alton Downs Basalt|68008|3|Fully described|p191, p251, p253-254, p267-270,p297,p465|Late Cretaceous|Late Cretaceous|Mapped and described by Kirkegaard et al. (1970). Alton Downs, NW of Rockhampton. The type area is 5km S of Alton Downs, where it forms a NE-trending ridge. Over 200m thick. Geochemistry detailed, and compared with Dalma Basalt: they may be the same unit. The c.67 Ma age is a minimum as it is from a weathered sample. Hosts a bright red iron-rich zone of uncertain thickness. Is assumed to form a bimodal assemblage with Mount Hedlow Trachyte.|67.3 +/- 2.6 Ma (K-Ar: Wellman, 1978).|||Overlies Rockhampton and Berserker Groups, Doonside and Mount Alma Formations; unconformably overlies Native Cat Andesite. Underlies Rossmoya beds. Surrounds (?is intruded by) Mount Hedlow Trachyte.|Black, generally non-vesicular (except for local flow-tops), alkali basalt, hawaiite and mugearite.|
40103|Alton Downs Basalt|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
40103|Alton Downs Basalt|68679|6|Mentioned|p312-313, p347|Cretaceous|Cretaceous|Northern New England Orogen.||||||
40103|Alton Downs Basalt|69594|5|Briefly described|p551-552, p559-560, p565|Late Cretaceous|Late Cretaceous|Overlies the Stanwell and Jim Crow Basins. Within-plate vulcanism. Has lithological and chemical similarities to the Dalma Basalt.||||May be part-equivalent to Dalma Basalt.|Olivine- and feldspar-phyric basalt.|
40103|Alton Downs Basalt|69952|6|Mentioned|p75|Late Cretaceous|Late Cretaceous|||||||
40103|Alton Downs Basalt|73450|6|Mentioned|p49-50, p52|||Flat-lying. Forms a bimodal assemblage with the Mount Hedlow Trachyte.||||||
75528|Alum Rock volcanics|65107|5|Briefly described|p287|Sakmarian|Sakmarian|Informal name. Age: SHRIMP U-Pb zircon 293.7+/-3.4 to 291.3+/-2.8 Ma. Also constrained by Terrica beds and Alum Rock Conglomerate (Permian).||||||
35059|Amarra Suite|23049|4|Described|p17|Early Devonian|Early Devonian|||||||
35059|Amarra Suite|23283|4|Described|p18|Devonian|Silurian|||||||
35059|Amarra Suite|23422|4|Described|p177|Middle Devonian|Early Devonian|See also Amarra Supersuite p216 Table 6.10.||||||
35059|Amarra Suite|23430|5|Briefly described|p484|||Lolworth Batholith Province||||||
35059|Amarra Suite|23508|5|Briefly described|Map Legend|Devonian|Silurian|||||||
35059|Amarra Suite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
35059|Amarra Suite|69592|4|Described|p292-293|Middle Devonian|Early Devonian|Comprises most of the Lolworth Batholith, Charters Towers Province. Medium-K to high-K, calc-alkaline, metaluminous to slightly peraluminous granites.|||Amarra, Myola, Davey Creek, Dillons Knob, Reedybed, Redlands, Weane Vale Granites.|Intrudes Cape River Metamorphics. Is intruded by Grasstree Suite.|Typically muscovite-biotite granites, with some minor garnet.|
35059|Amarra Suite|71966|5|Briefly described|p1006|Early Devonian|Early Devonian|Geological province: Charters Towers Province, Thomson Orogen. Of the Lolworth Batholith. Similar in age to Gumbardo Formation ignimbrites.||||||
36157|Amarra Supersuite|23422|4|Described|p216 Table 6.10|Early Devonian|Late Silurian|See also Amarra Suite (p20).||||||14-APR-08
36157|Amarra Supersuite|23505|5|Briefly described|Map legend|Devonian|Silurian|||||||
77808|Amber Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Porphyritic biotite granite.|
75644|Amelia Creek Tonalite|68679|5|Briefly described|p362-363, p366 Fig.5.57|Pennsylvanian|Pennsylvanian|Northern Connors Subprovince. Part of the Urannah Batholith. REE plot.|305.2 +/- 1.7 Ma (SHRIMP U-Pb: Cross et al., 2012)||||I-type.|
75644|Amelia Creek Tonalite|68901|5|Briefly described|p4, p77-p80, p146|Carboniferous|Carboniferous|New England Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|305.2 +/- 1.7 Ma (SHRIMP U-Pb)||||Pale grey, fine- to medium-grained, slightly uneven-grained hornblende-biotite quartz monzodiorite containing minor microcline and relatively coarse titanite.|15-NOV-18
75644|Amelia Creek Tonalite|69952|5|Briefly described|p89-90, p92|||SHRIMP U-Pb zircon age; also 304.3 +/- 5.8 Ma (Allen et al.,1998). These are both within uncertainty of the latest age determination of the Mount Crompton Granodiorite (Cross et al., 2015).|305.2 +/- 1.7 Ma (Cross et al., 2012).|||Is interpreted to intrude/cut the Mount Crompton Granodiorite.||
75644|Amelia Creek Tonalite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|306+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzodiorite.|
75644|Amelia Creek Tonalite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Pale grey to grey, medium to fine-grained, uneven-grained to moderately porphyritic biotite-hornblende tonalite to quartz monzodiorite; with minor titanite; generally weakly foliated, partly recrystallised.|
33149|Ametdale Volcanics|23042|4|Described|p21,30,8,45, 54, Fig 2|Early Permian|Late Carboniferous|Possible correlation to Mount Benmore and Lizzie Creek Volcanics.  Overlying unit Mount Buffalo Rhyolite. UInderlying unit Connors volcanics. Max. thickness 100 m.||||||
33149|Ametdale Volcanics|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Andesitic to basaltic lava and crystal rich volcanic sandstone, breccia and conglomerate.||||||17-SEP-04
33149|Ametdale Volcanics|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Andesitic to basaltic lava and crystal rich volcanic sandstone, breccia and conglomerate.||||||
33149|Ametdale Volcanics|61035|4|Described|p8|Early Permian|Late Carboniferous|Of the Lizzie Creek Volcanic Group. Overlain by Mount Buffalo Volcanics. Unit probably equlivalent to the Mount Benmore Volcanics. Geological Province: Connors Sudprovince.||||||07-FEB-11
33149|Ametdale Volcanics|65388|3|Fully described|p127-128, p90, 128, 85, 86, 90, 103|Early Permian|Early Permian|Of Lizzie Creek Volcanic Group. Originally included in Connors Volcanics. Ametdale Volcanics- mafic volcanics occur for 20km along eastern slopes of the Broadsound Range. A type section 1000m thick is designated. Overlie the Leura Volcanics, and are overlain by the Mount Buffalo Rhyolite [Volcanics]. May correlate with Mount Benmore Volcanics or alternatively the older Macksford Volcanics. Andesitic to basaltic volcaniclastic sandstone and conglomerate and some lava. See also  p110, 111, 124, 130, 132, 447.||||||
33149|Ametdale Volcanics|68679|4|Described|p353, p355, p357-358|||Connors Subprovince, Connors-Auburn Province. Previously mapped as part of the Connors Volcanics. Crops out over ~20km along the eastern edge of Broadsound Range. Has lithological and geochemical similarities with Mount Benmore Volcanics. Likely debris flow deposits.||Lizzie Creek Volcanic Group.||Overlies Leura Volcanics. Is overlain by Mount Buffalo Rhyolite [Volcanics]. May correlate with Mount Benmore Volcanics.|Trachyandesitic to basaltic volcaniclastic sandstone and conglomerate with some lava; poorly sorted and no bedding.|
82283|Amiens Leucomonzogranite|71628|4|Described|p12: 10; p15: 34-35, 43-46, 75-76,82,97|Middle Triassic|Early Triassic|See also p3: 102, 115. New name, after the locality of the same name. Extends 37 km from Sorrento almost to the Severn River NW of Ballandean; outcrop area c.197 km2. Crops out as large boulders, tors, whalebacks and extensive pavements in hilly country. Geochemistry detailed. Is spatially associated with several minor Sn deposits (named).||Amiens Suite.||Intrudes Passchendaele Monzogranite and Texas beds (and is faulted against the latter). Abuts Severn River, Benalla Monzogranites, Mount Norman Leucomonzogranite and Ruby Creek Leucogranite.|Pale pink to pale pinkish-grey, medium-grained, moderately porphyritic, leucocratic biotite (rarely amphibole-bearing) monzogranite to syenogranite; locally fine-grained and highly porphyritic. I-type.|
82284|Amiens Suite|71628|5|Briefly described|p15: 35, 43-44, 50, 75-76, 88|Middle Triassic|Early Triassic|||Stanthorpe Supersuite.|Amiens, Mount Norman Leucomonzogranites.|||
23334|Amity Aplite|22847|3|Fully described|p 50|Early Devonian|Late Silurian|||||||
23334|Amity Aplite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23334|Amity Aplite|42245|2|Defined|p40|Early Devonian|Late Silurian|||||||
23334|Amity Aplite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23334|Amity Aplite|43259|6|Mentioned|Appendix 1,p24.|Devonian|Silurian|of Emu Mill Granodiorite.||||||
23334|Amity Aplite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23334|Amity Aplite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Amity aplite.||||||
32074|Anabranch Basalt Flow|23509|5|Briefly described|Map Legend||Quaternary|Informal name.||||||
32074|Anabranch Basalt Flow|43933|5|Briefly described|Map Legend||Quaternary|||||||
32074|Anabranch Basalt Flow|73115|6|Mentioned|p: 76, 90, 94, 99, 105, 110, 115, 120|||See also Anabranch Basalt p75, 77||||||
36292|Ancaster Granite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36292|Ancaster Granite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|320-280 Ma.||||Hornblende-biotite granodiorite to biotite granite and leucogranite. I-type.|
30101|Anderson Creek Phyllite|22845|2|Defined|p7,18,32,34-6,77|Early Carboniferous|Late Devonian|Invalid name usage, Anderson Creek units already used elsewhere.||||||
30101|Anderson Creek Phyllite|22846|6|Mentioned|p14|||Invalid name as Anderson Creek units exist elsewhere predating this unit.||||||
30101|Anderson Creek Phyllite|43092|6|Mentioned|Fig.2|||Invalid name. Anderson Creek Formation already used in Vic.||||||
30101|Anderson Creek Phyllite|43588|6|Mentioned|p30||Late Devonian|||||||
30101|Anderson Creek Phyllite|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
30101|Anderson Creek Phyllite|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
30101|Anderson Creek Phyllite|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
30101|Anderson Creek Phyllite|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince. Polydeformed phyllite.||||||
30101|Anderson Creek Phyllite|68679|5|Briefly described|p325-326, p329-330, p334|Late Carboniferous|Late Devonian|Little et al. (1993). Kilkivan-Manumbar area, North D'Aguilar Subprovince. A thin, fault-bounded, polydeformed phyllitic unit forming a discontinuous slice <75m thick. Locally forms isolated klippen on ridge-tops. Detachment zone assemblage. Has a two-phase metamorphic and deformational history. Lithologically and structurally similar to Gobongo Metamorphics.||||Equivalent to Jimna Phyllite. Is faulted (possibly deposited) over Mount Mia Serpentinite. Is faulted under Amamoor beds, and partly overthrust by Claddagh Granodiorite.|Consists almost entirely of polydeformed pelitic phyllite, with rare fine-grained metapsammite beds. Lacks bedding or sedimentary features; has a micaceous sheen on cleavage surfaces.|
36279|Anglesey Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Bulleringa Volcanic Subgroup, Scardons Volcanic Group.||||||
36301|Angore Granite|23291|5|Briefly described|p44|Late Carboniferous|Carboniferous|See also Angore granite. Parent: O'Briens Creek Suite. Geological Province: Georgetown Region.||||||08-JUL-15
36301|Angore Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
36301|Angore Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Late Carboniferous age. Hydrothermally altered biotite granite, granite also included in 2 of the 3 subdivisions. ||Of the O'Briens Creek Supersuite.|Informally subdivided into three units based on grain size and geophysics.||Fine-grained biotite granite (porphyritic in part); pink to white, medium- to coarse-grained biotite granite (some fine-grained biotite granite and porphyritic biotite granite); variant of pink to white, medium to coarse, pink biotite granite?|
30693|Annable Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30693|Annable Granite|50536|5|Briefly described|p1.4, 8.2 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30693|Annable Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event.||Sybella Suite|||Granite.|
30693|Annable Granite|69591|6|Mentioned|p59|||Sybella Batholith.|||||Granite.|
28024|Annie Creek Schist|23420|5|Briefly described|p 145 table 4.4||Mesoproterozoic|In the Yambo Metamorphic Group, Yambo Subprovince. Age:~1580Ma||||||
28024|Annie Creek Schist|23429|5|Briefly described|p436|||||||||
28024|Annie Creek Schist|23496|5|Briefly described|Table 1||Proterozoic|Of Yambo Metamorphic Group. Age: ~1580Ma.||||||24-JUL-08
28024|Annie Creek Schist|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
28024|Annie Creek Schist|43596|4|Described|p10-11, p21 Tb. 1||Proterozoic|Of Yambo Metamorphic Group. Faulted against the Oswald Schist and Saraga Schist. Geological province: Yambo Inlier. Comprises metasediments (schist and quartzite) and myolitic two-mica granite. Further lithological detail presented (p21 Tb.1).||||||27-JAN-09
28024|Annie Creek Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|Yambo Metamorphic Group||||||24-JAN-05
28024|Annie Creek Schist|50537|5|Briefly described|p6.1|||Geological Province: Yambo Inlier.||||||
28024|Annie Creek Schist|69591|4|Described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Is intruded by the Cape York Peninsula Batholith.|~1577 Ma (two-mica granite).|Yambo Metamorphic Group.||Is faulted against Oswald and Saraga Schists.|Two-mica-sillimanite-garnet schist; psammitic schist; quartzite and amphibolite, mylonitic, medium-grained, two-mica granite.|
28024|Annie Creek Schist|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1642+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Crenulated mylonitic granite thrusting to west; mylonitic 2-mica granite.|
40104|Annie Creek beds|24615|5|Briefly described|CD|Jurassic|Triassic|[RJa].  Conglomerate, lithic sandstone, grey siltstone and carbonaceous shale.||||||
40104|Annie Creek beds|50197|5|Briefly described|Map Legend|Jurassic|Triassic|||||||
40104|Annie Creek beds|50214|5|Briefly described|Map Legend|Jurassic|Triassic|||||||
40104|Annie Creek beds|68008|2|Defined|p209, p226-228, p233|Early Jurassic|Late Triassic|New name, after Annie Creek, a tributary of Kroombit Creek. Previously mapped (Dear et al., 1971) as part of Precipice Sandstone. The reference section extends 100m up Annie Creek from near the junction with Hut Creek (GR02896 72928). Shallow lake deposits on an irregular volcanic landform: thickness varies from 7m to over 65m.||||Disconformably overlies Winterbourne Volcanics. Is overlain by Precipice Sandstone, locally gradationally.|Local thick beds of pebble and cobble conglomerate, interbedded with fine-grained grey sandstone, black carbonaceous shale, and grey siltstone which becomes dominant away from the conglomerate. Occasional grey lithic tuffs and thin cherty beds.|
40104|Annie Creek beds|68679|6|Mentioned|p338|Late Triassic|Late Triassic|New England Orogen.||||||
74639|Anniebrook Seam|22820|5|Briefly described|p30, p36 Fig. 14, p48 Appdx.1|Late Permian|Late Permian|This seam is a member of the Upper Permian Redgate Coal Measures, and is of high quality in the Rosa Brook area.||||||12-NOV-13
24162|Anning Granite|23032|5|Briefly described|p12|Proterozoic|Proterozoic|||||||
24162|Anning Granite|23220|5|Briefly described|Fig.2, p12|||Dykes cut Sawpit Granodiorite, Digger Creek Granite and Einasleigh Metamorphics. Forsayth Subprovince/GI.||||||
24162|Anning Granite|23291|4|Described|p89 Fig. 3.8|Early Devonian|Early Devonian|Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||18-JUN-15
24162|Anning Granite|23513|5|Briefly described|Map legend||Silurian|Palaeozoic Intrusive No. 65. I-Type.||||||
24162|Anning Granite|35920|2|Defined|p24|Devonian|Silurian|Late Proterozoic or Silurian to Devonian||||||
24162|Anning Granite|36937|6|Mentioned|p229|||||||||
24162|Anning Granite|37570|4|Described|p121|||||||||
24162|Anning Granite|37576|5|Briefly described|p8|||||||||
24162|Anning Granite|39445|6|Mentioned|p72|||See also P148||||||
24162|Anning Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24162|Anning Granite|43259|4|Described|Appendix 1,p19.|Early Devonian|Late Silurian|possibly Proterozoic.||||||
24162|Anning Granite|43664|6|Mentioned|p96|||||||||
24162|Anning Granite|50211|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pink to cream, locally weakly foliated, medium-grained biotite leucogranite. Age: 1550-1560 Ma. Of the Glenmore Batholith.||||||18-JUN-15
24162|Anning Granite|68357|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Glenmore Batholith, Pama Province.|||||Pink to cream, locally weakly foliated, medium-grained biotite leucogranite.|
24162|Anning Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
28185|Answer Slate|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Mary Kathleen Group.  Siltstone, slate, chert, sandstone, greywacke. Underlies Corella Formation. Overlies Overhang Jaspilite.||||||15-MAR-07
28185|Answer Slate|22460|5|Briefly described|p447|||Of the Mary Kathleen Group.||||||18-JUL-06
28185|Answer Slate|22461|5|Briefly described|Fig 1 p464|||Of the Mary Kathleen Group.||||||15-MAR-07
28185|Answer Slate|22747|6|Mentioned|Table1,p7|||Correlates with Corella Formation||||||
28185|Answer Slate|23064|6|Mentioned|135|||Geological  province: Mt Isa Inlier. Of Mary Kathleen Group.||||||15-MAR-07
28185|Answer Slate|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|||||||
28185|Answer Slate|23973|5|Briefly described|p1436|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Of the Mary Kathleen Group.||||||
28185|Answer Slate|23974|6|Mentioned|p1451 Fig. 1|||Geological Province: Mount Isa Inlier.||||||
28185|Answer Slate|24462|5|Briefly described|p296 Fig. 1|||||||||
28185|Answer Slate|29969|5|Briefly described|p392|||||||||
28185|Answer Slate|30530|6|Mentioned|p516|||||||||
28185|Answer Slate|30531|6|Mentioned|p15|||||||||
28185|Answer Slate|31704|6|Mentioned|p4|||||||||
28185|Answer Slate|32660|5|Briefly described|Table 5|||||||||
28185|Answer Slate|32959|6|Mentioned|Fig.21|||||||||
28185|Answer Slate|33900|6|Mentioned|p15|||See also P18||||||
28185|Answer Slate|34703|6|Mentioned|p23|||||||||
28185|Answer Slate|35074|6|Mentioned|Fig.2|||||||||
28185|Answer Slate|37862|4|Described|p587|||||||||
28185|Answer Slate|38234|6|Mentioned|Fig.2|||||||||
28185|Answer Slate|38235|6|Mentioned|p116|||||||||
28185|Answer Slate|38276|6|Mentioned|Fig.1|||||||||
28185|Answer Slate|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28185|Answer Slate|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group.||||||25-AUG-04
28185|Answer Slate|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28185|Answer Slate|39445|5|Briefly described|Table 2|||See also p36 and p43.||||||15-MAR-07
28185|Answer Slate|39496|4|Described|p9|||||||||
28185|Answer Slate|39622|6|Mentioned|Fig.2|||||||||
28185|Answer Slate|40840|6|Mentioned|Map legend|||||||||
28185|Answer Slate|41306|4|Described|p7|||||||||
28185|Answer Slate|41791|4|Described|p248|||||||||
28185|Answer Slate|41978|6|Mentioned|p491|||||||||
28185|Answer Slate|42166|6|Mentioned|p108|||||||||
28185|Answer Slate|44271|2|Defined|p30,56|||Conformably overlies Mitakoodi Quartzite. Probably contempory with lower part of Marimo Slate. Contains mineral deposits (Cu-Ag).||||||
28185|Answer Slate|44275|14|Not recorded|Map Legend|||||||||
28185|Answer Slate|44276|2|Defined|map,Tb.1,p11|||||||||
28185|Answer Slate|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
28185|Answer Slate|44279|14|Not recorded|Tb.1|||||||||
28185|Answer Slate|44290|2|Defined|p437||Paleoproterozoic|||||||07-NOV-08
28185|Answer Slate|44989|2|Defined|p.82|||Tb.III. Overlain by Staveley Formation. (F54-6). On many pages.||||||
28185|Answer Slate|45161|4|Described|p44|||||||||
28185|Answer Slate|45166|6|Mentioned|p29|||||||||
28185|Answer Slate|45287|14|Not recorded|p.225-227,229||Paleoproterozoic|||||||07-NOV-08
28185|Answer Slate|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
28185|Answer Slate|46962|4|Described|Table 1|||See also Fig.3.||||||
28185|Answer Slate|49009|1|Redefined|p3|Proterozoic|Proterozoic|||||||
28185|Answer Slate|50100|5|Briefly described|p11, p13 Fig. 4, p20|Proterozoic|Proterozoic|Metasiltstone, slate and phyllite; minor feldspathic quartzite, metagreywacke, chert, quartz-albite rock, marble, mica schist and quartz-hematite rock.  Intruded by Gin Creek Granite.  Geological Province: Eastern Fold Belt Province.  See also p49. ||||||
28185|Answer Slate|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier.||||||15-MAR-07
28185|Answer Slate|50536|6|Mentioned|p11.4|||Intruded by Gin Creek Granite.  Geological Province: Mount Isa Inlier.||||||
28185|Answer Slate|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Slate, phyllite, metasiltstone, mica schist.||||||
28185|Answer Slate|60658|5|Briefly described|p61, p62 Fig.1|Proterozoic|Proterozoic|Of the Mary Kathleen Group.||||||
28185|Answer Slate|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Isa Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||
28185|Answer Slate|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
28185|Answer Slate|61927|5|Briefly described|p92 Fig.1|||Geological Province: Mount Isa Inlier.||||||
28185|Answer Slate|61936|5|Briefly described|p190 Fig. 3|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
28185|Answer Slate|62047|6|Mentioned|p90 Fig.1 |||||||||
28185|Answer Slate|63866|5|Briefly described|p62|Statherian|Statherian|Potentially a deep water equivalent of the Gun Supersequence.|1652 +/- 16 Ma (Page, OZCHRON)|||||
28185|Answer Slate|64248|5|Briefly described|p36, p38 Fig.5|||Included in the informal Young Australia Group.|1652 +/- 16 Ma.|Mary Kathleen Group.||||11-DEC-17
28185|Answer Slate|64250|5|Briefly described|p14-15, p7, p11 fig 3, p20, p27|||Cloncurry Fold Belt, Mount Isa Inlier. Appears as Answer slate on p20.|1652 +/- 16 Ma (deposition)|Basal unit in Young Australia Group.||Merges laterally with Kuridala Formation.|Dominantly slate, siltstone and phyllite; commonly graphitic and pyritic; minor marble.|
28185|Answer Slate|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: between ~1680-1610Ma. Geological Province: Mount Isa Block.||||||
28185|Answer Slate|65387|4|Described|p1, p3 Tb.1, p22-28, p82-85|Statherian|Statherian|Also appears as Answer slate on p1. Maximum deposition (detrital zircon) age; this is consistent with an age of c.1652 Ma by Page (OZCHRON).|1654 +/- 11 Ma SHRIMP zircon (Carson et al. 2008)|Unit in Mary Kathleen Group.||Suggested correlation with Toole Creek Volcanics.|Includes fine-grained orange siltstone and a possible felsic tuff horizon.|
28185|Answer Slate|65396|5|Briefly described|p15-17, p82, p84, p169, p175, p178|Statherian|Statherian|See also p180-183, p188-190, p195, p202, p217, p241, p439. The authors propose grouping this and other siliciclastic units of the Mary Kathleen Group into the informal Young Australia Group, now part of the Mount Albert Group. Contains the Young Australia Mine. Isa Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. Has many lithological similarities to Kuridala Formation, and appears to merge laterally with it. Detrital zircon sources listed.|1675 - 1610 Ma, <1652 +/- 16 Ma.|Mary Kathleen Group||Overlies Roxmere Quartzite, Magna Lynn Metabasalt; conformably overlies Double Crossing Metamorphics. Is overlain by Staveley Formation. Is correlated with Kuridala Formation.|Slate, siltstone and phyllite; commonly graphitic and pyritic. Minor marble.|03-APR-17
28185|Answer Slate|66913|5|Briefly described|p170 fig 1, p172||||1690-1650 Ma|||Correlated with Marimo Slate, Toole Creek Volcanics.||
28185|Answer Slate|67323|4|Described|p18-20,  p26, 35,39, Solid Geology Map|||See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Marimo-Staveley and Kuridala-Selwyn Domains, Isa Superbasin. Includes rocks previously mapped as Marimo Slate and Agate Downs Siltstone. Low magnetic response.|1655 +/- 4 Ma (MDA: Carson et al., 2008).|Kuridala Group.||Is faulted against Double Crossing Metamorphics and Staveley Formation. Age-equivalent to Toole Creek Volcanics and Hampden Slate.|Mostly variably carbonaceous metapelitic rocks: slate, phyllite, metasiltstone, mica schist; minor feldspathic quartzite, chert.|
28185|Answer Slate|67539|5|Briefly described|p13|||Upper unit. Reassigned to include the Agate Downs Siltstone, Marimo Slate, and Answer Slate. ||Of the Kuridala Group.||Equivalent of the Toole Creek Volcanics? Underlain by the New Hope Sandstone?||
28185|Answer Slate|68146|5|Briefly described|p76|||Eastern Fold Belt, Mount Isa Inlier.||||Structurally overlies Double Crossing Metamorphics.||
28185|Answer Slate|68542|5|Briefly described|p16 fig 4, p17 fig 5||||||||Undifferentiated shale-slate and chloritic schist.|
28185|Answer Slate|68576|5|Briefly described|Q-2: p16-17|Proterozoic|Proterozoic|Part of Cover Sequence 3 (1690-1650 Ma) of the Eastern Fold Belt, Mount Isa Inlier.|||||Shale-slate and chloritic schist.|
28185|Answer Slate|68732|5|Briefly described|p162-163, p165 Fig.3, p168 Fig.5, p169|Statherian|Statherian|Hosts the Young Australia Mine. Detrital zircon maximum sedimentary depositional ages.|1652 +/- 16, 1654 +/- 11 Ma||||Monotonous intervals of massive to finely-laminated siltstone and shale, up to several hundred of metres thick.|30-NOV-17
28185|Answer Slate|69056|5|Briefly described|p55, Time-Space plot sheet|Statherian|Statherian|Marimo-Staveley Domain.|c.1655 - c.1652 Ma.|Kuridala Group.||||
28185|Answer Slate|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Overlies Kuridala Formation. Is overlain by Staveley Formation.||25-JAN-19
28185|Answer Slate|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert|
28185|Answer Slate|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert|
28185|Answer Slate|69591|4|Described|p43 Fig.2.31, p46, p49, p55, p108|||Marimo-Staveley Domain, Isa Superbasin. Includes rocks previously mapped as Marimo Slate and Agate Downs Siltstone. Part of Gun Supersequence. Deep-marine sediments. Forms an imbricate thrust belt of narrow, alternating linear belts with Staveley Formation. MDA by Carson et al. (2008).|1654 +/- 11 Ma (SHRIMP maximum depositional age).|Kuridala Group.||Coeval with Toole Creek Volcanics and (probably) Hampden Slate. Faulted against Staveley Formation.|Consists predominantly of variably carbonaceous metapelitic rocks: slate, phyllite, metasiltstone, mica schist; minor feldspathic quartzite, chert. Contains metadolerite sills.|
28185|Answer Slate|69952|5|Briefly described|p4, p51|||Maximum depositional age. Possible correlation with Hampden Slate.|<1660-1650 Ma (Carson et al., 2008, 2011).|Unit in upper part of Kuridala Group.||||
28185|Answer Slate|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert.|
28185|Answer Slate|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert.|
28185|Answer Slate|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Dark grey carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert. (Separately mapped) brown phyllite or fine-grained mica schist and graphitic slate.|
28185|Answer Slate|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Dark grey carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert. (Separately mapped) brown phyllite or fine-grained mica schist and graphitic slate.|
28185|Answer Slate|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Overlies Mount Albert Group. Probable equivalent to Hampden Slate.|Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert.|05-MAY-16
28185|Answer Slate|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Marimo-Staveley Domain, Doherty-Fig Tree Gully Domain.|||||Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schsit; minor feldspathic quartzite and chert.|
28185|Answer Slate|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1654+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone.|
28185|Answer Slate|71799|6|Mentioned|p160|||Eastern Fold Belt, Mt Isa.||||||
28185|Answer Slate|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain. Includes silicified fault zones, and brown phyllite.||||Probably unconformably overlies Agate Downs Siltstone. Intruded by unnamed metadolerite, metabasalt, amphibolite sills, shown as older than Wiggle Waterhole Metagabbro.|Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert. Includes siliceous and quartz-hematitic breccia and/or quartz mylonite. Brown phyllite or fine-grained mica schist and slate.|
28185|Answer Slate|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain. Includes silicified fault zones, and brown phyllite.||||Probably unconformably overlies Agate Downs Siltstone. Intruded by unnamed metadolerite, metabasalt, amphibolite sills, shown as older than Wiggle Waterhole Metagabbro.|Dark grey, carbonaceous slate, phyllite and metasiltstone grading into mica schist; minor feldspathic quartzite and chert. Includes siliceous and quartz-hematitic breccia and/or quartz mylonite. Brown phyllite or fine-grained mica schist and slate.|
28185|Answer Slate|72889|6|Mentioned|p8.|||||||||
28185|Answer Slate|73525|6|Mentioned|p4-5 Fig.2|||Kuridala-Selwyn-Marimo-Doherty Domain.|||||Carbonaceous shale (-silt) siliciclastics.|
23339|Ant Hill Andesite Member|23291|4|Described|p92 Fig. 3.9|Early Permian|Late Carboniferous|Parent: Ironhurst Formation of the Maureen Volcanic Group. Thickness: 50-120m. Geological Province: Georgetown Region.||||||08-JUL-15
23339|Ant Hill Andesite Member|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Ironhurst Formation, Maureen Volcanic Group.||||||
23339|Ant Hill Andesite Member|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23339|Ant Hill Andesite Member|40542|6|Mentioned|p97|||||||||
23339|Ant Hill Andesite Member|43259|6|Mentioned|Appendix 1,p1.||Carboniferous|||||||
23339|Ant Hill Andesite Member|43740|6|Mentioned|Fig.5,p45|||||||||
23339|Ant Hill Andesite Member|50595|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Ironhurst Formation. Underlies: Womblealla Rhyolite Member.||||||01-JUL-04
23339|Ant Hill Andesite Member|68352|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Maureen Cauldron. Strongly magnetic. Min Age: Early Permian?||Unit in Ironhurst Formation.||Is overlain conformably by Womblealla Rhyolite Member.|Dark greenish grey, aphyric augite-basaltic andesite; possibly includes intrusive equivalents.|18-MAY-15
27974|Aralba Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group.||||||31-JUL-08
27974|Aralba Granite|23496|5|Briefly described|Table 2, p39|Devonian|Silurian|Of Aralba Suite ( Kintore Supersuite).||||||31-JUL-08
27974|Aralba Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Aralba Suite.||||||31-JUL-08
27974|Aralba Granite|43596|4|Described|p30, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite).  Intrudes Oswald and Saraga Schists. Strongly/abundantly porphyritic biotite-muscovite granite + abundant muscovite and K-feldspar phenocrysts.||||||15-JAN-09
27974|Aralba Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
27974|Aralba Granite|70207|5|Briefly described|p72|||Cape York Peninsula Batholith. Unit in Pama Igneous Association.|400 +/- 5 Ma (Rb-Sr: Cooper et al., 1975).|Kintore Supersuite.||||
29752|Aralba Suite|23420|4|Described|p 151 table 4.8||Early Devonian|Also see p 147 table 4.6. In the Kintore Supersuite.||||||
29752|Aralba Suite|23496|5|Briefly described|Table 2, p39|Devonian|Silurian|Of Kintore Supersuite.||||||31-JUL-08
29752|Aralba Suite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
29752|Aralba Suite|43596|4|Described|p30, p26 Tb. 2, p28 Tb. 3|||Of the Kintore Supersuite. Contains Top Pinnacle, Lilyponds, Kingvale, Kopo, Chevy Creek, Wongu, Kokomini, Aralba and Laia Granites. Named from the Aralba Adamellite of Willmott et al (1973).||||||27-JAN-09
29752|Aralba Suite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of the Kintore Supersuite||||||31-JUL-08
27670|Aranbanga Volcanic Group|23037|6|Mentioned|p116||Triassic|||||||
27670|Aranbanga Volcanic Group|23799|3|Fully described|p106, p10 Tb. 1|Late Triassic|Late Triassic|Supersedes "Aranbanga beds". Overlain(u) by Oakdale Sst. and Main Range Volcs; underlain(u) by Fifer Cr Metamorphics. Intruded by Toondahra Granite, Canoe Ck. Granite and Wooroonden Granodiorite.  Geol.Prov: South-east Qld.Volcanic and Plut. Province.||||||14-AUG-08
27670|Aranbanga Volcanic Group|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
27670|Aranbanga Volcanic Group|24279|5|Briefly described|p1800,1803, 1804|Late Triassic|Late Triassic|Age: 214-234 Ma. Overlies Toogoolawah Group and Curtis Island Group.||||||
27670|Aranbanga Volcanic Group|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
27670|Aranbanga Volcanic Group|41736|6|Mentioned|p115|||||||||
27670|Aranbanga Volcanic Group|41738|1|Redefined|p169|Late Triassic||||||||
27670|Aranbanga Volcanic Group|41778|6|Mentioned|Fig.1|||||||||
27670|Aranbanga Volcanic Group|41790|5|Briefly described|p474|||||||||
27670|Aranbanga Volcanic Group|41917|6|Mentioned|p524|||||||||
27670|Aranbanga Volcanic Group|42054|6|Mentioned|p273|||||||||
27670|Aranbanga Volcanic Group|43008|5|Briefly described|map legend|||||||||
27670|Aranbanga Volcanic Group|43092|5|Briefly described|p31|||||||||
27670|Aranbanga Volcanic Group|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
27670|Aranbanga Volcanic Group|44923|5|Briefly described|Map Legend||Late Triassic|||||||
27670|Aranbanga Volcanic Group|50320|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
27670|Aranbanga Volcanic Group|60371|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Rhyolitic to dacitic lava and pyroclastic deposits locally intercalated with volcanogenic sediments.||||||
27670|Aranbanga Volcanic Group|61772|6|Mentioned|p129, p130 Fig. 5||Late Triassic|In New England Orogen.||||||14-AUG-08
27670|Aranbanga Volcanic Group|63821|4|Described|p19, p21, p37|Late Triassic|Late Triassic|Unconformably overlies Toogoolwah Group. Age: 221+/-4Ma. Geological Province: Esk Trough. Formed a sheet of generally flat-lying volcanics, not subsequently folded but have been affected by major faulting.||||||07-FEB-11
27670|Aranbanga Volcanic Group|64398|5|Briefly described|Map legend|Late Triassic|Middle Triassic|Age: Middle Triassic? - Late Triassic?  Aphyric or sparsely phyric rhyolite.||||||
27670|Aranbanga Volcanic Group|65388|6|Mentioned|p206|||Found to SE of study area. Correlated with Mount Eagle Volcanics.||||||
27670|Aranbanga Volcanic Group|65452|5|Briefly described|p2-5, p35-37|Late Triassic|Late Triassic|Features post-caldera eruption of mafic to intermediate lavas. See individual units for ages. Occupies Mungore Cauldron and Gayndah Centre; is "associated" with Mungore Granite. Mafic to intermediate volcanism followed by significant periods of voluminous silicic magmatism and development of large caldera system. Thought to represent extension-related magmatism.|226 - 214 Ma.||Includes Abernethy Basalt.||Rhyolitic ignimbrite and lavas associated with caldera collapse. Basalts and andesites above and below? rhyolites, extensive late-stage subvolcanic intrusive complex.|
27670|Aranbanga Volcanic Group|66855|6|Mentioned|p955.|||||||||
27670|Aranbanga Volcanic Group|67203|6|Mentioned|p2-3, p36-37|Late Triassic|Late Triassic|Stephens (1991). Associated with caldera complex. Requires further geochronological work for comparison with Mount Marcella Volcanics.||||||
27670|Aranbanga Volcanic Group|67874|5|Briefly described|p2-3, p7-8, p11, p19, p34, p43-46|Late Triassic|Late Triassic|Widespread, silicic-dominated unit. Is associated with the Mungore Caldera. Previous K-Ar dates ranged from ~221 to ~224 Ma. This study shows this unit is significantly older than a previously reported K-Ar age of 172.2 +/- 2.2 Ma. SHRIMP U-Pb zircon magmatic crystallisation age.|229.7 +/- 1.4 Ma (Cross et al., 2012).||Includes Johngboon Rhyolite.|Is intruded by Mungore Granite.|Includes lithic-bearing ignimbrites, and rhyolitic lava domes and cryptodomes.|06-NOV-15
27670|Aranbanga Volcanic Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the North Arm Volcanic Group; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
27670|Aranbanga Volcanic Group|68679|4|Described|p312-313, p326, p387, p391, p413, p420|Late Triassic|Late Triassic|See also p429-430, p434, p436-437, p439-441, p469, p472. North D'Aguilar Subprovince, northern New England Orogen. Comagmatic with Mungore Granite and its associated un-named granites in the Mungore Cauldron. CONSTITUENTS described in detail pp439-440, including numerous un-named units and subunits. Hosts porphyry and epithermal style mineralisation (e.g. the Mount Rawdon gold mine).|||Woodmillar Andesite; Abernethy, Wetheron Basalts; Beeswing, Johngboon, Dadamarine Rhyolites.|Overlies Boondooma Igneous Complex; Mount Marcella Volcanics; Wigton, Chowey and Mingo Granites. Is intruded by Toongahra and Mungore Granites.|Undifferentiated andesite and rhyolite lavas and domes, basaltic to rhyolitic volcanics, volcaniclastic sediments and tuffs, epiclastic sediments.|
27670|Aranbanga Volcanic Group|71592|5|Briefly described|Appendix A.|||New England Orogen.|||||Rhyolite.|
27670|Aranbanga Volcanic Group|72297|5|Briefly described|p710|||Intrudes coeval interbedded subaerial pyroclastic flow, surge and ashfall deposits associated with the Mount Rawdon gold deposit.|||||Dacite.|
27670|Aranbanga Volcanic Group|73450|4|Described|p3-4, p24-25, p29-30, p32-35|Carnian|Carnian|Crops out extensively in a broad N-NW trending belt in the Goomeri-Mount Perry region. Comprises many geological units and subunits and covers a wide compositional spectrum. Interpreted as genetically related to the Mungore Granite (Stephens, 1991). Hosts epithermal gold mineralisation at Mount Rawdon. K-Ar age of 224.2 +/- 3.2 Ma from Mount Lawless (Stephens, 1991). U-Pb SHRIMP zircon age of 229.7 +/- 1.4 Ma (Cross et al., 2012).|ca 230 Ma||Woodmillar Andesite, Beeswing Rhyolite, Wetheron Basalt|Underlain by Mount Marcella Volcanics. Intruded by Hogback Granite and Mungore Granite. Equivalent to Dadamarine Rhyolite and Ooramera Volcanics.|Bimodal alkaline magmatism.|
23340|Arch Creek Limestone Member|23032|5|Briefly described|p25 fig6||Early Devonian|||||||
23340|Arch Creek Limestone Member|23430|5|Briefly described|p504|||Shield Creek Formation. Graveyard Creek Subprovince.||||||
23340|Arch Creek Limestone Member|41260|5|Briefly described|p48|||||||||
23340|Arch Creek Limestone Member|41679|2|Defined|p253|Pragian|Lochkovian|||||||
23340|Arch Creek Limestone Member|41719|6|Mentioned|Fig.2|||||||||
23340|Arch Creek Limestone Member|41740|6|Mentioned|p222|||||||||
23340|Arch Creek Limestone Member|42031|5|Briefly described|p760|||||||||
23340|Arch Creek Limestone Member|42032|5|Briefly described|p495|||||||||
23340|Arch Creek Limestone Member|42054|6|Mentioned|p273|||||||||
23340|Arch Creek Limestone Member|42933|4|Described|p76|||of Shield Creek Formation||||||
23340|Arch Creek Limestone Member|44447|6|Mentioned|p135|Early Devonian|Early Devonian|Of the Shield Creek Formation.||||||
23340|Arch Creek Limestone Member|65214|6|Mentioned|p275|Devonian|Devonian|QLD, Broken River. Appears in text as Arch Ck Limestone Member. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23340|Arch Creek Limestone Member|69030|5|Briefly described|p6|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province).||Shield Creek Formation.||||
23340|Arch Creek Limestone Member|69592|5|Briefly described|p263-264|Pragian|Lochkovian|Lang et al. (1989). A richly fossiliferous lens in the Wade Anticlinorium.||Shield Creek Formation.||||
77810|Arden Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Hornblende-biotite granite.|
27312|Ardroy Tuff Member|34261|2|Defined|p97|Middle Triassic|Middle Triassic|Previously equated with Linville Tuff||||||
78843|Argyle seam package|65096|5|Briefly described|p372, p376 Fig.5|Middle Jurassic|Middle Jurassic|[informal 'sequence stratigraphy' unit] Comprises a single fining upwards cycle with a wireline signature of interbedded coals and shales. Also written as Argyle seam on p372. See also fig.2, p370.||Said to be of the Juandah Coal Measures sequence.||Equivalent in part to Tangalooma Sandstone and lower Juandah Coal Measures. Overlain by Iona seam package.||
31445|Argylla Suite|24197|5|Briefly described|p27, p93|Paleoproterozoic|Paleoproterozoic|Mainly extrusive comprising volcanics of Argylla and Bottletree Formations, and the intrusive Bowlers Hole Granite and Mairindi Creek Granite. Predominantly a volcanic suite. Age: 1810-1746Ma. Geol.Prov: Mount Isa Inlier. Eg.of the Sybella Association.||||||07-FEB-11
31445|Argylla Suite|50100|6|Mentioned|p17|Proterozoic|Proterozoic|Includes the Argylla Formation.||||||
31445|Argylla Suite|50536|5|Briefly described|p1.2, 1.4, 4.1 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1780Ma.||||||07-NOV-08
31445|Argylla Suite|67497|5|Briefly described|p890 Fig.2, p909|Statherian|Statherian|Geochemistry and age (1775+/-6 Ma determined using SHRIMP U-Pb zircon analysis) from sample FBMI-6510 given.|1780 - 1740 Ma (Wilson et al. 1984).||Includes Argylla Formation, Mairindi Creek Granite, Bowlers Hole Granite.||Pinkish-grey porphyritic rhyolite and dacite.|07-MAY-12
31445|Argylla Suite|72596|6|Mentioned|p1, p49|||Of Budd et al. (2001).|||Includes Bowlers Hole Granite, felsic igneous rocks of the Argylla Formation.|||
31445|Argylla Suite|73525|6|Mentioned|p20|||Mary Kathleen Domain. See also Argylla Formation.||||||
31445|Argylla Suite|73553|5|Briefly described|p46, p64||||||Argylla Formation, Bowlers Hole Granite, Mairindi Creek Granite|||
28028|Arkara Gneiss|23291|5|Briefly described|p22|||Geological Province: Coen Region.||||||
28028|Arkara Gneiss|23420|5|Briefly described|p 145 table 4.4||Proterozoic|In the Yambo Metamorphic Group, Yambo Subprovince. Age:~1580Ma||||||
28028|Arkara Gneiss|23429|5|Briefly described|p436|||Also see p437.||||||
28028|Arkara Gneiss|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group. Age: ~1575 - 1585Ma(SHRIMP).||||||
28028|Arkara Gneiss|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
28028|Arkara Gneiss|43596|4|Described|p13, p21 Tb. 1|Mesoproterozoic|Mesoproterozoic|Of Yambo Metamorphic Group.  Age: 1575Ma (U-Pb SHRIMP). Variably deformed (mylonitic), dark grey, medium- to coarse-grained, garnet-muscovite-biotite granodiorite.  Detailed lithology presented ( p21 Tb. 1).||||||07-APR-15
28028|Arkara Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|Age: 1581+/-8 Ma. Yambo Metamorphic Group||||||24-JAN-05
28028|Arkara Gneiss|50537|5|Briefly described|p6.2|Mesoproterozoic|Mesoproterozoic|Age: 1575Ma (SHRIMP). Intrudes Yambo Metamorphic Group.||||||07-APR-15
28028|Arkara Gneiss|63866|5|Briefly described|p79|||||||||
28028|Arkara Gneiss|69591|4|Described|p70, p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Coen Inlier. Numerous small outcrops in the metasedimentary units. Comparable in age to the (c.1585 Ma) Cardross Orthogneiss.|1584 +/- 2 Ma.|Yambo Metamorphic Group.||May partly correlate with Daintree Gneiss.|Variably deformed (mylonitic), garnet-muscovite-biotite granodiorite to monzogranite locally highly porphyritic or megacrystic.|
28028|Arkara Gneiss|71592|5|Briefly described|Appendix A.|||Etheridge Province. Metamorphosed at 1576 +/- 5 Ma (U-Pb zircon SHRIMP).|1581+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodioritic gneiss.|
24667|Armagh Limestone|34252|6|Mentioned|Ps.16|||Fossils||||||
37925|Arra Granite|23291|6|Mentioned|p101 Tb. 3.12|Late Carboniferous|Late Carboniferous|Intruded by Charles Knob granite. Geological Province: Georgetown Region.||||||08-JUL-15
37925|Arra Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Claret Creek Supersuite.|||Mainly (muscovite-) biotite granite.|
23342|Arrabury Formation|13497|4|Described|iv, viii, xii, p69 fig 6.1, p102|Early Triassic|Late Permian|Cooper Basin. Defined by Powis (1989) as the basal unit of the Nappamerri Group and a type section was deisgnated also. Maximum thickness of 400m in the Patchawarra Trough. Seals the Toolachee Formation and forms a regional seal over all the Permian formations of the basin. Wireline log results are discussed. See also p104-p106, p108, p110, p112, p114, p119, p125, p127, p165-p166, p169-p174, p179.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Conformably overlies the Toolachee Formation. Unconformably overlies the Innamincka Formation. Conformably overlain by the Tinchoo Formation. Disconformably overlain by the Hutton Sandstone.|Dark to pale grey siltstone and mudstone beds with interbedded pale-grey and cross-bedded sandstones.|
23342|Arrabury Formation|13516|5|Briefly described|p171 fig 12|Early Triassic||In Eromanga Basin.|||Includes Callamurra Member, Wimma Sandstone Mmember|||
23342|Arrabury Formation|22839|6|Mentioned|P33|Early Triassic|Late Permian|||||||
23342|Arrabury Formation|22883|6|Mentioned|P29|Early Triassic|Late Permian|Underlying unit is Toolachee Formation||||||
23342|Arrabury Formation|23154|5|Briefly described|Map Legend|Triassic|Permian|Geological Province - Cooper Basin. Parent - Nappamerri Group.||||||16-FEB-10
23342|Arrabury Formation|23155|4|Described|p23 & Fig 13 on p24|Mesozoic|Mesozoic|Contains a sparse unusually oxidised pollen assemblage indicative of a Late Permian to Early Triassic age.||||||
23342|Arrabury Formation|23375|4|Described|Fig2 p265,283|Spathian|Dzhulfian|In the Cooper Basin.||||||17-JAN-08
23342|Arrabury Formation|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Late Permian|Of the Nappamerri Group. Includes the Callamurra and Paning Members and the Wimma Sandstone Members. Geological Province: Cooper Basin.||||||16-FEB-10
23342|Arrabury Formation|42008|2|Defined|p269|Anisian|Tatarian|See also Fig.2, Fig.3||||||
23342|Arrabury Formation|42085|6|Mentioned|Fig.2 P374|||||||||
23342|Arrabury Formation|43052|5|Briefly described|Table 2.1|||||||||
23342|Arrabury Formation|44133|4|Described|p65 Fig. 8.3, 85|Triassic|Permain|Of the Nappamerri Group. Geological Province: Cooper Basin. Includes: Callamurra Member, Paning Member, Wimma Sandstone Member. Overlies: Toolachee Formation .||||||17-JAN-08
23342|Arrabury Formation|60386|6|Mentioned|p299|Early Triassic|Early Triassic|Cooper/Eromanga Basin. Non-marine.||||||
23342|Arrabury Formation|60717|5|Briefly described|p40 Fig. 2|Anisian|Tatarian|Of Nappamerri Group. Contains Callamurra and Paning Members, and Wimma Sandstone Member. Overlies Toolachee Formation; overlain by Tinchoo Formation. Combined thickness = 375m. Geological Province: Cooper Basin.||||||31-JAN-08
23342|Arrabury Formation|61613|5|Briefly described|p282 Fig. 2|Triassic|Late Permian|Of Nappamerri Group. Includes Callamurra, Paning and Wimma Sandstone Members. Overlain by Tinchoo Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
23342|Arrabury Formation|61614|6|Mentioned|p290 Fig. 2|Middle Triassic|Late Permian|Of Nappamerri Group. Geological Province: Cooper Basin.||||||17-MAR-09
23342|Arrabury Formation|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Late Permian|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
23342|Arrabury Formation|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Of Nappamerri Group. Includes Wimma Sandstone, Paning and Callamurra Members. Geological Province: Cooper Basin.||||||
23342|Arrabury Formation|62537|6|Mentioned|p191 Fig.2. |Middle Triassic|Early Triassic|Cooper Basin.||Unit in Nappamerri Group.|Includes Wimma Sandstone, Callamurra and Paring Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|62730|5|Briefly described|p352 Fig. 1|Late Triassic|Late Permian|Of the Nappamerri Group. Includes the Callamurra Member. Geological Province: Eromanga Basin.||||||21-APR-08
23342|Arrabury Formation|63978|2|Defined|p7, p19, Fig. 3|Early Triassic|Late Permian|Basal unit of Nappamerri Group. Includes the Wimma Sandstone, Paning and Callamurra Members. Conformably overlies Toolachee Fm. Unconformably overlies Innamincka Fm. (Warburton Basin). Max. thick: 412m. In Cooper Basin. Detailed lithology included.||||||07-FEB-11
23342|Arrabury Formation|64048|5|Briefly described|p64 Tb. 2|Early Traissic|Late Permian|Basal unit of the Nappamerri Group. Contains the Callamurra, Paning and Wimma Sandstone Members. Unconformably overlain by Tinchoo Formation.  Geological Province:Cooper Basin.||||||07-FEB-11
23342|Arrabury Formation|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Late Permian|||Nappamerri Group|Includes Callamurra, Paning, and Wimma [Sandstone], Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Early Triassic|Cooper Basin.|||Includes Callamurra, Paning, and Wimma Sandstone, Members.|Overlies Toolachee Formation. Is overlain by Tinchoo Formation.||
23342|Arrabury Formation|65238|5|Briefly described|p9|Triassic|Triassic|Geological province: Cooper Basin. Red bed succession in sedimentary continuum with the underlying Toolachee Formation. Unconformably underlies Tinchoo Formation.||||||17-FEB-10
23342|Arrabury Formation|65489|5|Briefly described|p15, p48-49, p55, p96, p131-132|Early Triassic|Early Triassic|Cooper Basin. Gas and oil reservoir accounting for 1% each of the Basin's production. Regional seal. Shown as Tatarian to Anisian on p48.||Unit in Nappamerri Group.|Includes Callamurra, Paning, and Wimma Sandstone, Members.|Overlies Toolachee Formation (Gidgealpa Group). Is overlain by Tinchoo Formation. Probably equivalent to Walkandi Formation.||
23342|Arrabury Formation|65925|5|Briefly described|Appendix 2.||||||||Red beds, sandstone, siltstone, mudstone carbonaceous in part. Fluvial, fluvio-lacustrine.|
23342|Arrabury Formation|67402|6|Mentioned|p90, p90 fig CPR4, p91, p92|||||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Unconformably overlain by the Tinchoo Formation. Overlies the Gidgealpa Group.||
23342|Arrabury Formation|68731|4|Described|p200 Fig 3.110, pp208-211|Anisian|Lopingian|Cooper Basin. ~ 420-200 m thick. Deposition was on a vegetated flood plain with ephemeral lakes in lowland areas and pedogenesis in exposed areas. Palynological dating indicates a late Lopingian-early Anisian age (Gray and McKellar 2002).||Basal unit of the Nappamerri Group.|Includes the Callamurra Member, Paning Member, and the Wimma Sandstone Member.|Conformably underlain by the Toolachee Formation. Unconformably overlain by the Tinchoo Formation.|Comprises interbedded sandstone, siltstone and mudstone with some redbed characteristics. Siderite occurs as speckles, diffuse layers and as patchy cement.|02-JUL-14
23342|Arrabury Formation|69454|5|Briefly described|p38:4|Anisian|Changhsingian|Cooper Basin. Appears as Arrabury Sandstone on 38:8.||Nappamerri Group.||Correlated with Walkandi Formation (Pedirka Basin).||12-JUL-16
23342|Arrabury Formation|69673|6|Mentioned|p153 fig 125|||||Nappamerri Group||Overlain by Tinchoo Formation, overlies Toolachie Formation||
23342|Arrabury Formation|69728|6|Mentioned|p285|||Cooper Basin.||Nappamerri Group.||||
23342|Arrabury Formation|69797|5|Briefly described|p17 Fig.2|Middle Triassic|Late Permian|Age: Tatarian - Anisian (approximated from figure). Geol. Prov: Cooper Basin.||Nappamerri Group|Wimma Sandstone Member, Paning Member, Callamurra Member|||
23342|Arrabury Formation|69946|5|Briefly described|p9, p36, p54, p68|Early Triassic|Permian|Cooper Basin. Tatarian to Anisian.||Unit in Nappamerri Group.|Includes Paning, Wimma Sandstone and Callamurra Members.|Conformably overlies Toolachee Formation. Is overlain conformably by Tinchoo Formation.||
23342|Arrabury Formation|69947|5|Briefly described|p13 Fig.7.2|Early Triassic|Permian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|||
23342|Arrabury Formation|69982|5|Briefly described|p44, p62, p68|Triassic|Triassic|Hydrocarbon shows from the Warburton Basin rocks have been incorrectly assigned to this unit (and others). Brief thin section descriptions.|||||Redbeds.|
23342|Arrabury Formation|70317|5|Briefly described|p33|Middle Triassic|Late Permian|Cooper Basin. Lacustrine, flood plain depositional environment.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|Overlies Toolachee Formation. Is overlain by Callamurra Member (Arrabury Formation).||
23342|Arrabury Formation|70823|4|Described|iv, p40, p70,|Olenekian|Late Permian|Cooper Basin. Deposited in braided fluvial, floodplain or lacustrine environments. Distribution, outcrop and palynological characteristics are discussed briefly. This unit is generally 200 to 350m thick in the Nappamerri Trough and between 380 to 390m thick in the Arrabury Trough. Hosts a commercial reservoir. See also p75-p76, p78-p79, p81-p82.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Conformably overlies the Toolachee Formation. Unconformably overlies the Warburton Formation.  Conformably overlain by the Tinchoo Formation.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
23342|Arrabury Formation|70824|4|Described|p7-p9, p104|Olenekian|Induan|Cooper Basin. Up to 400m thick.||Nappamerri Group|Includes the Callamurra Member, Paning Member and the Wimma Sandstone Member.|Overlies the Toolachee Formation. Overlain by the Tinchoo Formation.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds overlain by sandstone with minor siltstone interbeds.|
23342|Arrabury Formation|70946|5|Briefly described|p1089|Middle Triassic|Permian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning, Wimma Sandstone, Members.|Overlies the Toolachee Formation. Overlain by the Tinchoo Formation.||08-OCT-18
23342|Arrabury Formation|71265|5|Briefly described|p589|Induan|Olenekian|Cooper Basin.||Nappamerri Group.|Callamurra, Paning Members.|Overlies Toolachee Formation.||
23342|Arrabury Formation|71342|5|Briefly described|Ch5 p9, Ch5 p31, Ch5 p36|Anisian|Tatarian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial, floodplain or lacustrine environment. See also Ch5 p54, Ch5 p67, Ch7 p13.||Nappamerri Group|Includes the Paning, Wimma Sandstone and the Callamurra Members.|Conformably overlies the Toolachee Formation.||
23342|Arrabury Formation|71701|4|Described|p155|Olenekian|Induan|Cooper Basin.||Nappamerri Group|Includes the Paning and Callamurra members.|Overlies the Toolachee Formation.||
23342|Arrabury Formation|72297|5|Briefly described|p742|||Cooper Basin.|||Callamurra Member.|||
23342|Arrabury Formation|73251|6|Mentioned|p62|Middle Triassic|Permian|Cooper Basin. Braided fluvial channel belt, floodplain, lacustrine, and moderately sinuous fluvial channel depositional environments.||Nappamerri Group|Wimma Sandstone Member, Paning Member, Callamurra Member|Underlain by Toolachee Formation (Gidgealpa Group). Overlain by Tinchoo Formation.||
27036|Arrongulla Formation|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Inorunie Group.||||||
27036|Arrongulla Formation|23291|4|Described|p83 Tb. 3.6|Early Paleozoic|Mesoproterozoic|Parent: Inorunie Group. Thickness: 300m? Geological Province: Georgetown Region.||||||08-JUL-15
27036|Arrongulla Formation|40218|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
27036|Arrongulla Formation|40954|6|Mentioned|p132|||||||||
27036|Arrongulla Formation|41975|6|Mentioned|Fig.3 P433|||||||||
27036|Arrongulla Formation|43664|6|Mentioned|Fig.3,p15|||||||||
27036|Arrongulla Formation|68355|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Guela Sandstone.|Dark red-brown, variably ferruginous laminated micaceous lithic-quartz siltstone and fine sandstone; mudstone; minor shale, fine- to medium-grained orthoquartzite.|
27036|Arrongulla Formation|68356|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Guela Sandstone.|Dark red-brown, variably ferruginous laminated micaceous lithic-quartz siltstone and fine sandstone; mudstone; minor shale, fine- to medium-grained orthoquartzite.|
27036|Arrongulla Formation|69591|6|Mentioned|p75|||Croydon Province, Georgetown Inlier.||Inorunie Group.||||
36374|Arrow Sandstone Formation|23425|5|Briefly described|p373 Fig 9.10|||Of Pascoe River Group.||||||
27999|Artella Granite|23420|4|Described|p 152 table 4.8||Early Devonian|Intrudes Burton Lagoon Granite and Pine Tree granite.||||||
27999|Artella Granite|43596|5|Briefly described|p34, p28 Tb. 3|||Muscovite-biotite granite, unassigned.||||||15-JAN-09
27999|Artella Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
27945|Artemis Granodiorite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
27945|Artemis Granodiorite|22781|4|Described|p27|Paleozoic|Paleozoic|Flyspeck Supersuite||||||07-NOV-08
27945|Artemis Granodiorite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Kintore Granite. Age: 406+/-10Ma||||||
27945|Artemis Granodiorite|42610|3|Fully described|p24|Early Devonian|Late Silurian|Age 406 +/-10Ma. Formerly incl. in Flyspeck Granodiorite & "Kintore Adamellite" B135.||||||
27945|Artemis Granodiorite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Penny and Kimba Gneisses. medium-grained allanite-biotite granodiorite to monzogranite; porphyritic in part.||||||15-JAN-09
27945|Artemis Granodiorite|43738|6|Mentioned|Fig.12,p38|||||||||
27945|Artemis Granodiorite|69592|5|Briefly described|p282|||Cape York Peninsula Batholith.|406 +/- 10 Ma (SHRIMP U-Pb zircon).|Flyspeck Supersuite.||||
27945|Artemis Granodiorite|73387|5|Briefly described|p29|Early Devonian|Early Devonian|Zircon U-Pb (SHRIMP) age of 406 +/- 10 Ma from Black et al. (1992). I-type granite.|406 +/- 10 Ma U-Pb SHRIMP|Flyspeck Supersuite||||20-DEC-22
36520|Artillery Hill microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 170.||||||
30375|Arundel Rhyolite|22675|4|Described|p78|Early Permian|Early Permian|Age: ~293Ma||||||05-AUG-08
30375|Arundel Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V77. I-Type.||||||
30375|Arundel Rhyolite|43259|5|Briefly described|Appendix 1,p8||Late Carboniferous|Of Bulgonunna Volcanic Group.||||||05-AUG-08
30375|Arundel Rhyolite|43391|5|Briefly described|Map legend||Late Carboniferous|Of the Bulgonunna Volcanic Group.  Rhyolitic ignimbrites.  Geological Province: Coastal Ranges Igneous Province.||||||23-JUN-04
30375|Arundel Rhyolite|43727|5|Briefly described|Table 14,p50|||||||||
30375|Arundel Rhyolite|43734|6|Mentioned|p6|||U-Pb age: 293.5+/-5.6 Ma||||||
30375|Arundel Rhyolite|60659|5|Briefly described|p16|Early Permian|Early Permian|Of Bulgonunna Gp. Lower moderately crystal-poor to crystal-rich, welded to locally unwelded rhyolitic ignimbrite, with minor flow-banded rhyolite - and upper unit of massive welded rhyolitic ignimbrite. Age: ~293Ma. Of the Bulgonunna Province.||||||07-FEB-11
30375|Arundel Rhyolite|69593|4|Described|p495, p513|Permian|Late Carboniferous|Burdekin Falls Subprovince, Kennedy Igneous Association. The LITHOLOGY description is for the whole Group. Sm-Nd isotope data tabulated.|294 +/- 6 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments. I-type.|
30375|Arundel Rhyolite|70740|5|Briefly described|p8, p81, p82 fig 50, p84|Early Permian|Early Permian|SHRIMP age derived from Black (1994). At least 200m thick in places. See also p87, p106, p109.|293.5 +/- 5.6 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Overlies the Smedley Dacite and Star of Hope Formation.|Rhyolitic ignimbrite.|
36247|Askins Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||05-AUG-08
36247|Askins Microgranite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Slightly porphyritic biotite microgranite; included in Pinnacles Granite on most recent maps. I-type.||||||07-FEB-11
26356|Aspley Formation|40579|6|Mentioned|Map legend|late Carnian|late Carnian|||||||
26356|Aspley Formation|40623|5|Briefly described|p7|||||||||
26356|Aspley Formation|42316|5|Briefly described|p18|||||||||
26356|Aspley Formation|43076|5|Briefly described|p7|||||||||29-SEP-05
26356|Aspley Formation|68679|5|Briefly described|p394|||Ipswich Basin: Brisbane/Beenleigh/offshore.||||Equivalent to Mount Crosby Formation.||
27697|Atlanta Granite|23423|5|Briefly described|p305 Table 7.3|||||||||
27697|Atlanta Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~303 Ma, Rb-Sr. of  O'Briens Creek Supersuite.||||||
27697|Atlanta Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: ~303 Ma Rb-Sr.||||||
27697|Atlanta Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 245. I-Type.||||||
27697|Atlanta Granite|23616|6|Mentioned|Table 3 p44|||||||||
27697|Atlanta Granite|29820|6|Mentioned|p450|||||||||
27697|Atlanta Granite|33205|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27697|Atlanta Granite|39445|6|Mentioned|p90|||Blake(1972)||||||
27697|Atlanta Granite|42547|6|Mentioned|p75|||||||||
27697|Atlanta Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Breins Creek Supersuite).  Pale grey, very strongly porhyritic, fine to coarse biotite granite. Age: 302Ma.||||||15-JUN-06
27697|Atlanta Granite|43259|4|Described|Appendix 1,p33.||Carboniferous|Age is 302 Ma.||||||
27697|Atlanta Granite|43626|6|Mentioned|p10||Late Carboniferous|||||||
27697|Atlanta Granite|45065|4|Described|Table 4|||||||||
27697|Atlanta Granite|45113|3|Fully described|p16|||Emphasis on petrography.||||||
27697|Atlanta Granite|46845|6|Mentioned|Table 1|||||||||
27697|Atlanta Granite|46879|6|Mentioned|Fig.1|||||||||
27697|Atlanta Granite|60425|4|Described|p45 Tb. 3, p49 Tb. 3, p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supersuite).Age: ~303Ma (Rb-Sr). Unconformable below or faulted against Walsh Bluff Volcanics; intruded Boonmoo Volcanic Subgp of Featherbed Volcanic Group. Highly porphyritic biotite granite - more lith details incl.||||||07-FEB-11
27697|Atlanta Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pale grey, very highly porphyritic to uneven-grained, medium- to coarse-grained biotite granite; minor aplite, pegmatite; rare small mafic enclaves.|
27697|Atlanta Granite|72983|6|Mentioned|p1, p18|Gzhelian|Kasimovian|Age is corrected K-Ar biotite age (Richards et al., 1966). Unit was also dated using Rb-Sr, which yielded a similar age.|303 Ma K-Ar|||Intruded by Collins Weir Rhyolite.||
80230|Auburn Seam|68117|5|Briefly described|p347-349, p351-352, p354 Fig.11|Middle Jurassic|Middle Jurassic|Surat Basin. Topmost coal seam; locally absent. Coal analysis.||Taroom Coal Measures.||||
80230|Auburn Seam|71282|5|Briefly described|p456, p457 Fig.1, p466 Fig.13|||This, and the other eight named coal seams in the Walloon Subgroup, are presented as "coal-seam groups" with the authors making the totally unjustified claim they were "following the nomenclature of Scott et al. (2007)". [The term does not appear anywhere in the 2007 article.]||Taroom Coal Measures.||||
80230|Auburn Seam|72297|5|Briefly described|p699 Fig.10.11|Jurassic|Jurassic|Surat Basin.||Taroom Coal Measures.||||
75737|Augustus Igneous Complex|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p9|Statherian|Statherian|New unit. Camooweal - Murphy Domain, Mount Isa Inlier. Forms basement to Isa and Calvert Superbasins. Recognised from drilling.|~1700 Ma||||Altered granite (?originally marginally peralkaline) intrudes comagmatic fluorine-bearing rhyolite.|
75737|Augustus Igneous Complex|69591|5|Briefly described|p40, p59|||Alkaline to possibly peralkaline complex, comprising altered granite and comagmatic volcanics.|1705 +/- 8 Ma (Curtin Uni. Tech., unpub. data).|||Intrudes Corella or Quilalar Formations.|Grey strongly porphyritic metarhyolite; dark grey, equigranular Na-rich rock, possibly peralkaline granite with granophyric textures; magnetite-rich skarn.|
26358|Aurora Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Forsayth Supersuite. Geological Province: Georgetown Region.||||||24-JUN-15
26358|Aurora Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 821. S-Type.||||||
26358|Aurora Granite|24197|5|Briefly described|p17, p79 tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Age: ~1550Ma. Geological province: Georgetown Inlier.||||||07-FEB-11
26358|Aurora Granite|34883|6|Mentioned|p85|||||||||
26358|Aurora Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
26358|Aurora Granite|36216|6|Mentioned|p208|||||||||
26358|Aurora Granite|37570|4|Described|p119|||||||||
26358|Aurora Granite|38366|6|Mentioned|p34|||||||||
26358|Aurora Granite|39687|6|Mentioned|p3|||||||||
26358|Aurora Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26358|Aurora Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||05-AUG-08
26358|Aurora Granite|50537|5|Briefly described|p1.2, 1.4, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.||||||
26358|Aurora Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Muscovite-biotite leucogranite.||||||01-JUL-04
26358|Aurora Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Pale grey, fine- to medium-grained muscovite-biotite leucogranite.|
26358|Aurora Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith.||Forsayth Supersuite.|||Irregular, equigranular to porphyritic granite plutons (as well as veins and dykes) with small phenocrysts.|
24673|Aurukun Surface|24032|6|Mentioned|p29|||||||||
24673|Aurukun Surface|24033|5|Briefly described|p3|||Equlivalent to the Tennant Creek Surface.||||||
24673|Aurukun Surface|37607|5|Briefly described|Fig.3|||See also p333.||||||02-FEB-09
24673|Aurukun Surface|39556|5|Briefly described|Map legend|Oligocene|Oligocene|||||||
24673|Aurukun Surface|39899|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
24673|Aurukun Surface|40000|6|Mentioned|p254|||||||||
24673|Aurukun Surface|42650|5|Briefly described|p18|||||||||
24673|Aurukun Surface|64820|4|Described|pS7|Mid-Tertiary|Early Tertiary|Predominant land surface on Weipa Plateau - defined by Grimes (1979) after Doutch (1976). Overlies Bulimba Formation. At Weipa, covered with bauxite, but in some areas by 'ferruginous laterite'. ||||||
24673|Aurukun Surface|69599|5|Briefly described|p584-586, p602, p650|Oligocene|Eocene|On plains bordering Gulf of Carpentaria and Cape York Peninsula. Contemporary with Tennant Creek Surface to the SW.|||||Deep laterites and sporadic silcretes.|
31367|Avoca Creek Granodiorite|22845|6|Mentioned|Fig6|Triassic|Permian|||||||
31367|Avoca Creek Granodiorite|22846|2|Defined|p6,35-7|Middle Triassic|Late Permian|Contains 3 distinct phases.||||||
31367|Avoca Creek Granodiorite|43588|6|Mentioned|p31|Early Triassic|Late Permian|||||||
31367|Avoca Creek Granodiorite|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Porphyritic hornblende granodiorite.||||||
31367|Avoca Creek Granodiorite|65668|5|Briefly described|p2 Tb.1, p22-25|Triassic|Triassic|Gympie area; New England Orogen. Fine-grained porphyritic hornblende-biotite granodiorite; quartz porphyry; fine- to medium-grained biotite-hornblende granodiorite. Age: 235.4 +/-2.3 Ma (SHRIMP U-Pb zircon); significantly younger than the age of 255 +/- 5 Ma (K/Ar hornblende) obtained by Grayson (1995). Intrudes Bryden Formation.||||||
31367|Avoca Creek Granodiorite|68679|5|Briefly described|p391, p409, p411|Late Triassic|Late Triassic|Along the E margin of the Esk Basin, northern New England Orogen. A NNW-trending sill ~15km long. Distinctive by its low magnetic response and porphyritic rock types.|235.4 +/- 2.2 Ma (SHRIMP U-Pb: Cross et al. 2009).|||Intrudes Neara Volcanics and Marumba beds.|Porphyritic hornblende granodiorite.|
31367|Avoca Creek Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|235+/-2.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
23348|Awring Granodiorite|9531|5|Briefly described|Map Legend|Permian|Carboniferous|Hornblende-biotite granodiorite.||||||02-JUL-04
23348|Awring Granodiorite|23291|5|Briefly described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Western Georgetown Region. Age: ca.280Ma. Geological Province: Georgetown Region.||||||08-JUL-15
23348|Awring Granodiorite|23430|5|Briefly described|p493|||Kidston Subprovince. Kennedy Province.||||||
23348|Awring Granodiorite|23431|5|Briefly described|p531|||I-type.||||||
23348|Awring Granodiorite|23453|5|Briefly described|p12 Tab.1|Early Permian|Early Permian|281+/-3Ma||||||
23348|Awring Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 2. I-Type.||||||
23348|Awring Granodiorite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
23348|Awring Granodiorite|40659|6|Mentioned|p250|||||||||
23348|Awring Granodiorite|40860|4|Described|p110|||||||||
23348|Awring Granodiorite|40954|6|Mentioned|p132|||||||||
23348|Awring Granodiorite|43259|4|Described|Appendix 1,p15.||Permian|K-Ar age is 281+/-3 Ma. Rb/Sr age is 276+/-4 Ma.||||||
23348|Awring Granodiorite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Hornblende-biotite granodiorite, biotite granodiorite to tonalite, fine biotite leucogranodiorite; altered in part, some disseminated chalcopyrite.|
23348|Awring Granodiorite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Hornblende-biotite granodiorite, biotite granodiorite to tonalite, fine biotite leucogranodiorite; altered in part, some disseminated chalcopyrite.|
23348|Awring Granodiorite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Western Georgetown region. Unassigned.|||||I-type. Hornblende-biotite and biotite granodiorite (to tonalite), biotite granite; some dolerite.|
23348|Awring Granodiorite|70207|5|Briefly described|p4, p11, p13-18|Permian|Permian|Western part of the Georgetown Inlier (North Australian Craton). Unit in the Kennedy Igneous Association. Crops out as low bouldery ridge, isolated boulders and pavement. This U-Pb zircon age determination is within uncertainty of K-Ar and Rb-Sr ages by Mackenzie (1987).|279.2 +/- 2.7 Ma (Kositcin et al., 2015).||||Pale grey, fine-grained, slightly altered, porphyritic hornblende-biotite quartz monzodiorite? with sparse, euhedral plagioclase phenocrysts and quartz ocelli; occasional rapakivi texture.|
23348|Awring Granodiorite|71592|5|Briefly described|Appendix A.||||279+/-2.7 Ma (SHRIMP U-Pb zircon).||||Granodiorite.|
36275|Aylesbury Microgranite|23291|5|Briefly described|p97 Tb. 3.11|Early Permian|Early Permian|Of Brodies Camp Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
36275|Aylesbury Microgranite|23510|5|Briefly described|Map Legend||Early Permian|Of Brodies Camp Supersuite.||||||05-AUG-08
36275|Aylesbury Microgranite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Brodies Camp Supersuite.|||A-type.|
24167|B Creek Rhyolite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Overlies the Goat Creek Basalt; overlain by Parrot Camp Rhyolite.||||||14-APR-15
24167|B Creek Rhyolite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group.||||||
24167|B Creek Rhyolite|23510|5|Briefly described|Map Legend||Mesoproterozoic|of Croydon Volcanic Group.||||||
24167|B Creek Rhyolite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V802. S-Type.||||||
24167|B Creek Rhyolite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24167|B Creek Rhyolite|40659|2|Defined|p252|Mesoproterozoic|Mesoproterozoic|||||||
24167|B Creek Rhyolite|40954|6|Mentioned|p132|||||||||
24167|B Creek Rhyolite|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24167|B Creek Rhyolite|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24167|B Creek Rhyolite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Rhyolitic ignimbrite, dacitic ignimbrite, tuff, breccia; minor andesite.||||||14-APR-15
83683|BG3 Seam|73305|6|Mentioned|p553 Fig.5, p555, p556 Tb.3, p559|Late Permian|Late Permian|Northern Bowen Basin. Previously unnamed coal seam, 7.8 to 38 m thick, typically separate from the overlying Girrah Seam in the Burngrove Formation. See also p558 Fig.10.||Burngrove Formation|||Coal seam.|
81480|BG4 Seam|70861|6|Mentioned|p40,42-43|Late Permian|Late Permian|Of Bowen Basin.||Of Burngrove Formation.||||29-AUG-19
81481|BG5 Seam|70861|6|Mentioned|p40,42-43|Late Permian|Late Permian|Of Bowen Basin.||Of Burngrove Formation.||||29-AUG-19
36368|Badu Suite|23421|4|Described|Tb 5.3 p164|||Intrudes Torres Strait Volcanic Group. 'Badu' means igneous.||||||
36368|Badu Suite|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as parts of the Almaden, Ingham, Leichhardt, O'Briens Creek and Ootann Supersuites, and various ungrouped Carboniferous-Early Permian plutonic units, are all mapped under the symbol, CPgk.||||||
36368|Badu Suite|69593|4|Described|p476-477|||Torres Strait region: Jardine Subprovince, Kennedy Igneous Association. High-level (miarolitic) intrusives and associated volcanics. K-Ar age determinations by Richards and Willmott (1970) and von Gnielinski et al. (1997).|~300-285 Ma.||Torres Strait Volcanic Group, Badu Granite, Horn Island Granite.||Microgranite, biotite granite, hornblende-biotite granite, biotite-hornblende granodiorite, lithic and/or crystal-rich, rhyolitic and dacitic ignimbrite and other volcanic rocks. Locally common tonalitic to granodioritic enclaves.|
36368|Badu Suite|71031|5|Briefly described|p3, p39, p43|Early Permian|Late Carboniferous|Appears as Badu Supersuite on p3 and p43.|294-303 Ma K-Ar (von Gneilinski et al, 1997)|||||
83359|Badu Supersuite|71031|6|Mentioned|p3, p43|||See also Badu Suite p39.||||||
83359|Badu Supersuite|72983|6|Mentioned|p4|||Jardine Subprovince, Kennedy Igneous Association.|||Endeavour Strait Ignimbrite, Torres Strait Volcanic Group|||
26361|Bagstowe Granite|23032|4|Described|p44||Early Carboniferous|||||||
26361|Bagstowe Granite|23291|4|Described|p46, p97 Tb. 3.11|Carboniferous|Carboniferous|Of the Glenmore Supersuite. Intrudes the Paddock Creek Formation. Intruded by Eastdale Granite. Geological Province: Georgetown Region.||||||18-JUN-15
26361|Bagstowe Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 38. I-Type.||||||
26361|Bagstowe Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26361|Bagstowe Granite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
26361|Bagstowe Granite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
26361|Bagstowe Granite|43664|6|Mentioned|p96|||||||||
26361|Bagstowe Granite|43740|4|Described|p27||Carboniferous|||||||
26361|Bagstowe Granite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
26361|Bagstowe Granite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Overlies Black Cap Microdiorite.||||||14-MAY-04
26361|Bagstowe Granite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province. In Northeast Stock and Central Ring Dyke of the Bagstowe Ring Structure.|||||Pink, fine-grained biotite granite and microgranite.|
26361|Bagstowe Granite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Pink, fine-grained biotite granite and microgranite.|
26361|Bagstowe Granite|69593|4|Described|p488|||Kidston Subprovince, Kennedy Igneous Association. Is locally mixed with Black Cap Diorite.|~345-335 Ma (SHRIMP U-Pb zircon ages).|Glenmore Supersuite.|||(Hornblende-)biotite and biotite granite; locally strongly miarolitic; some accessory topaz and fluorite; local mixing with adjacent mafic rocks. I-type.|
33928|Baileys monzodiorite|22465|6|Mentioned|p934-5|||Informal name||||||
33142|Bajool Quartz Diorite|23799|5|Briefly described|p117|||Of Dumgree Suite.  Geological Province: Yarrol Province.||||||
33142|Bajool Quartz Diorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgaj].  Hornblende quartz diorite.||||||
33142|Bajool Quartz Diorite|50208|5|Briefly described|Map Legend|Triassic|Permian|||||||
33142|Bajool Quartz Diorite|68008|2|Defined|p28-29, p393-395, p484, p486, p622-624|Triassic|Permian|New name. These granitic rocks were first noted by Reid (1943), and mapped as unnamed Permian granodiorite by Kirkegaard et al. (1970). Named after the town of Bajool. The unit extends 18 x 15 km from Bajool to Mount Bomboola. Deeply weathered; outcrops are rare. The type area is a small quarry at GR266300 7372800 on the Bajool 100k sheet, and surrounding area. Forms very flat topography. Geophysics modelled, geochemistry described. Three circular quartz pipes up to 73m diameter are sources of lump silica.|249 +/- 5 Ma (K-Ar on sericite).|||Intrudes Mount Warner Volcanics; Mount Alma, Raspberry Creek Formations; Ginger Creek and Erebus beds; Rockhampton Group, and Mount Dick beds (which it contact metamorphoses).|Equigranular, medium-grained quartz diorite: 72% plagioclase (andesine), 25% hornblende, 2% quartz and 1% opaques. Post-tectonic.|
33142|Bajool Quartz Diorite|68679|5|Briefly described|p315, p423-425, p427|||Yarrol belt. Forms a narrow, N-S strip ~12 x 4 km. Magnetic data, geochemistry briefly discussed.|249 +/- 5 Ma (K-Ar sericite: QA148/LH1-Green 1975)|||Intrudes Mount Warner Volcanics, Raspberry Creek Formation, Erebus beds, Mount Alma Formation, Rockhampton Group, Mount Dick beds (Capella Creek Group).|Hornblende quartz diorite. May have concentric compositional variation.|
36455|Bakers Blue Granite|23423|5|Briefly described|p252||Early Permian|Age: 280 +/- 2 Ma (Rb-Sr). Yates Supersuite.||||||
36455|Bakers Blue Granite|23430|5|Briefly described|p495|||||||||
36455|Bakers Blue Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 389.  I-Type.||||||
36455|Bakers Blue Granite|50387|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Kennedy Province. Age: 280 +/- 2 Ma (Rb-Sr). Of Yates Supersuite||||||11-JUN-04
36455|Bakers Blue Granite|60425|4|Described|p91, p272-3 Appdx. 1|Early Permian|Early Permian|Of Bakers Blue Suite (Yates S'suite). Age: 280+/-2Ma (Rb-Sr whole rock biotite). Med.- fine-grained, even-gr.to slightly porph. hornblende-biotite granite, I-type; scattered microgranite inclusions to ~10cm; accessory zircon, ilmenite, apatite, allanite.||||||07-FEB-11
36455|Bakers Blue Granite|69593|5|Briefly described|p480, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 +/- 2 Ma.|Yates Supersuite.|||I-type.|
69326|Bakers Blue Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Yates Supersuite. Contains Bakers Blue Granite. I-type. Age: 280+/-2Ma (Rb-Sr).||||||07-FEB-11
27700|Bakerville Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Almaden Supersuite. Age: 302+/-5Ma Rb-Sr.||||||
27700|Bakerville Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 251. I-Type.||||||
27700|Bakerville Granodiorite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
27700|Bakerville Granodiorite|29820|6|Mentioned|p450|||||||||
27700|Bakerville Granodiorite|33205|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
27700|Bakerville Granodiorite|36527|6|Mentioned|p162|||||||||
27700|Bakerville Granodiorite|39445|6|Mentioned|p90|||Blake(1972)||||||
27700|Bakerville Granodiorite|40860|6|Mentioned|p113|||||||||
27700|Bakerville Granodiorite|42547|5|Briefly described|p75|||||||||
27700|Bakerville Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Kalunga Suite (Almaden Supersuite). Age: 301+/-5Ma.||||||15-JUN-06
27700|Bakerville Granodiorite|43259|4|Described|Appendix 1,p33.||Late Carboniferous|Age is 301+/-5 Ma.||||||
27700|Bakerville Granodiorite|45065|4|Described|Table 4|||||||||
27700|Bakerville Granodiorite|45113|3|Fully described|p14|||Emphasis on petrography.||||||
27700|Bakerville Granodiorite|46845|6|Mentioned|Table 1|||||||||
27700|Bakerville Granodiorite|46879|6|Mentioned|Fig.1|||||||||
27700|Bakerville Granodiorite|48976|4|Described|p40|||Isotopic data Table 9||||||
27700|Bakerville Granodiorite|60425|4|Described|p282-3 Appdx.|Early Permian|Late Carboniferous|Of Kalunga Suite (Almaden Supersuite).Age:301+/-5Ma, 298Ma (Rb-Sr).Med. to dk.grey, med.- to fine-grained, even-grained to slightly porphyritic biotite-hornblende (minor) + hornblende-biotite granodiorite; rare aplite,aplitic biotite microgranite. I-type||||||07-FEB-11
32040|Balaclava Formation|23468|5|Briefly described|p 296|||||||||
32040|Balaclava Formation|24399|5|Briefly described|p275, p272 Fig. 1|Late Devonian|Late Devonian|Volcaniclastic sediments, minor limestone and varying proportions of primary volcanic rocks.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt.||||||
32040|Balaclava Formation|24491|4|Described|p18|Late Devonian|Late Devonian|Supersedes Pond Formation.||||||
32040|Balaclava Formation|24615|5|Briefly described|CD|Early Carboniferous|Late Devonian|[DCb].  Rhyolitic volcaniclastic sandstone and conglomerate, minor ignimbrite, rare rhyolite, siltstone and oolitic limestone.||||||
32040|Balaclava Formation|50197|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32040|Balaclava Formation|50208|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32040|Balaclava Formation|50215|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Rhyolitic volcaniclastic sandstone and conglomerate, minor ignimbrite, rare rhyolite, siltstone and oolitic limestone.||||||18-JUN-09
32040|Balaclava Formation|50317|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Rhyolitic volcaniclastic sandstone and conglomerate, minor ignim,brite, rare rhyolite, siltstone and oolitic limestone.||||||09-JUN-04
32040|Balaclava Formation|60282|5|Briefly described|p9|Late Devonian|Late Devonian|Includes the former Pond Formation. Geological Province: Yarrol Province.||||||
32040|Balaclava Formation|61035|6|Mentioned|p12|Early Carboniferous|Late Devonian|Geological Province: Yarrol Province.||||||07-FEB-11
32040|Balaclava Formation|61392|5|Briefly described|p165 Fig. 2|Famennian|Frasnian|Part of the 'Bindawallah Stratigraphic Assemblage'.||||||07-FEB-11
32040|Balaclava Formation|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Late Devonian|Geological Province: Yarrol Province. See also p1000 Fig.3, p1027.||||||
32040|Balaclava Formation|65388|6|Mentioned|p72|||Correlated with Tanderra Volcanics.||||||
32040|Balaclava Formation|68008|2|Defined|p40, p42, p50, p61, p67-71, p77, p79-80|Tournaisian|Frasnian|See also p90-91, p109, p131, p378, p381, p479, p573, p580-581, p588-592, p597-598, p628, p648, p652. Established to include the oldest strata displaying an increased radiometric response resulting from the Carboniferous-to-Devonian change to more felsic volcanic rocks. Includes the former Pond Formation, parts of the Capella Creek Group, and other undivided rocks. Forms a discontinuous SE-trending belt. The type section, which does not include the base nor top of the Formation, is at GR254331 7352785 in the Bajool 100k sheet. Measured type section diagram. Forms hilly topography. Geochemistry discussed; discrimination plots. About 2000m thick. Age from diverse brachipood fauna (listed). The base is highly diachronous. Hosts small garnetiferous skarn deposits, some with minor base metals, associated with Sawnee Gabbro. Micropaleontology table. Shelly fossils listed; locations. Geophysics modelling.  At least partly equivalent to Mount Hoopbound and Lochenbar Formations and Three Moon Conglomerate. May be intruded by Pomegranate Tonalite.||||Unconformably overlies Ginger Creek Member. Is overlain conformably by Rockhampton Group and unconformably by Youlambie Conglomerate. Is intruded by Sawnee Gabbro and Rocky Point Granodiorite.|Dominantly sandstone and granule to pebble conglomerate; lesser ignimbrite; rare siltstone, oolitic limestone and rhyolite lava. Lithologies described in some detail.|
32040|Balaclava Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Lochenbar and Mount Hoopbound Formations, the Tanderra Volcanics,  the Channer Creek beds and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
32040|Balaclava Formation|68679|5|Briefly described|p312-313,p338-339,p348,p403 Tb.5.8,p425|Tournaisian|Frasnian|Northern New England Orogen. Combines the Pond Formation (Maxwell, 1953) with some undivided Late Devonian of Kirkegaard et al. (1970) and Dear et al. (1971). The siltstones are fossiliferous; oolitic limestone near the top of the Formation is identical with basal Rockhampton Group.||||Is intruded by Rocky Point Granodiorite, Eulogie Park and Sawnee Gabbros, and Kyle Mohr Igneous Complex. May correlate with Tanderra Volcanics.|Mainly feldspatholithic to lithofeldspathic sandstones, poorly sorted, usually thick, may be tuffaceous; granule to pebble conglomerate with volcanic clasts. Less abundant are rhyolitic ignimbrite and lava, oolitic limestone and siltstone.|
40846|Balcooma Metavolcanic Group|50200|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
40846|Balcooma Metavolcanic Group|50201|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
40846|Balcooma Metavolcanic Group|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|||||||
40846|Balcooma Metavolcanic Group|67455|4|Described|p575 Table 1, p576, p577. |Early Ordovician|Late Cambrian|Early Paleozoic metavolcanic and metasedimentary succession trending NNE. Equivalent to the Seventy Mile Range Group in the Charters Towers Province. Amphibolite facies contains andalusite, staurolite and garnet in addition to widespread biotite. Hosts Balcooma massive-sulfide deposit.|471 +/- 4 Ma (U-Pb zircon: Withnall et al. 1991).||Includes Clayhole Schist.||Massive pelite and quartzose metasandstone, overlain by massive metarhyolitic volcaniclastics with prominent metarhyolite in west, some metadolerite and meta-andesite.|
40846|Balcooma Metavolcanic Group|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.|||Includes Clayhole Schist.|||
40846|Balcooma Metavolcanic Group|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.|||Includes Clayhole Schist.|||
40846|Balcooma Metavolcanic Group|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province. Also includes an un-named metadolerite.|||Includes Clayhole Schist; Dry River and Highway Metavolcanics; Golden Creek Meta-andesite, and Lochlea Metarhyolite.|||
40846|Balcooma Metavolcanic Group|68346|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian||||||Mica schist and quartzite.|
40846|Balcooma Metavolcanic Group|68410|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Contains 3 unnamed subunits.|||||Mica schist, quartzite and gneiss; intervals of leucogneiss (meta-rhyolite?) and amphibolite; muscovite and biotite leucogneiss and granofels; mica schist and quartzite, grading into gneiss, some leucogneiss and granofels.|
40846|Balcooma Metavolcanic Group|68553|6|Mentioned|Map legend|Early Ordovician|Cambrian|||||||
40846|Balcooma Metavolcanic Group|68576|5|Briefly described|Q_11: p33|Early Ordovician|Late Cambrian|Hosts significant VHMS deposits, mined at Balcooma.||||Correlated with the Seventy Mile Range Group. Is intruded by the Dido Tonalite.|A suite of deformed, amphibolite facies felsic volcanics and sedimentary rocks, and metabasalt. Includes porphyritic metarhyolite, very fine-grained metasandstone and muscovite schist with andalusite porphyroblasts.|
40846|Balcooma Metavolcanic Group|68731|5|Briefly described|p152, p154, p155, p159, p189, p220, p122|Early Ordovician|Early Ordovician|An age of 480 +/- 4 ma was obtained by Rea (2000). Black and Harvey (1991) reported an age of 471 +/- 4 Ma from an intrusive porphyry. Reflects a deep- to shallow-marine succession with common volcaniclastic sedimentation and associated volcanic and intrusive activity.|480 +/- 4 Ma; 471 +/- 4 Ma||Includes Clayhole Schist, Dry River Metavolcanics, Golden Creek Meta-andesite, Lochlea Metarhyolite, and Highway Metavolcanics.|Intruded by the Ringwood Park Microgranite and the Dido Tonalite. Correlative of the Seventy Mile Range Group.|Includes biotite and muscovite leucogneiss derived from rhyolitic volcanic and tuffaceous rocks as well as high-level felsic intrusions.|04-MAY-15
40846|Balcooma Metavolcanic Group|70744|5|Briefly described|p939, p947|||Greenvale Province. U-Pb zircon age by Withnall et al. (1991). Appears also as Balcooma Metavolcanics on p939. Buried, shortened and exhumed by the Benambran Orogeny. Age of 480-470 Ma (Fergusson and Henderson, 2013). Metamorphosed c.443-425 Ma (Ali, 2010).|c.470 Ma (estimated from Fig.7).||||Amphibolite facies metamorphic rocks.|
40846|Balcooma Metavolcanic Group|70749|5|Briefly described|p42-43|Ordovician|Ordovician|Greenvale Province.|480 +/- 4 Ma.||||Mainly felsic metavolcanic and metasedimentary sequences representing back arc basin deposits.|
40846|Balcooma Metavolcanic Group|71592|5|Briefly described|Appendix A.|||Thalanga Base Metal Metallogenic Province. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|507+/-22 Ma and 471+/-4 Ma.||||Porphyry.|
40846|Balcooma Metavolcanic Group|71966|5|Briefly described|p989-990,999|Tremadocian|Tremadocian|Geological province: Greenvale Province, Thomson Orogen. Magmatism associated with the 490-460 Ma Larapinta extensional event.  Hosts significant Cu-Pb-Zn-Au-Ag bearing volcanic massive sulfide style deposits. Geochronological ages include SHRIMP U-Pb age of 480+\-4 Ma (Rea, 2000; cited in Jell, 2013).|480+\-4 Ma|||||
40846|Balcooma Metavolcanic Group|72297|5|Briefly described|p718, p721|Paleozoic|Paleozoic|Greenvale Province. Hosts the Balcooma VMS deposit in the eastern part of the Georgetown Inlier. A quartzite ridge SSW of Conjuboy homestead contains widespread kyanite and andalusite, with several lesser minerals (listed).|||||Bimodal but predominantly felsic volcaniclastics and lavas; metapelite lenses within a meta-arenite sequence hosts VMS mineralisation.|
40846|Balcooma Metavolcanic Group|73425|6|Mentioned|p18|||Greenvale Province, Thomson Orogen.|480 +/- 4 Ma.|||||
73063|Bald Hill Formation|61392|4|Described|p163-165, p167|Early Devonian|Early Devonian|Of the Silverwood Group (Keinjan Terrane). Divided into Units A, B and C. Age: 389-386 Ma [probably from 1995 timesscale]. Max. thickness: 2450m.||||||03-SEP-18
73063|Bald Hill Formation|63731|5|Briefly described|Map legend|Devonian|Silurian|Of Silverwood Gp. Volcaniclastic arenite+siltstone, basaltic to andesitic lavas; arenite+mudstone with chert; basaltic debris flow deposits, metabasite sills+hybassyl intrusions; metagabbro, lenses of limestone+marble; pepperites; polymictic paraconglom.||||||19-AUG-08
73063|Bald Hill Formation|63748|4|Described|p7 Fig. 3, p8|Emsian|Pragian|Of Silverwood Group. Unconformable on Connolly Volcanics; conformably overlain by Ormoral Volcanics. Max. thickness: ~2450m. Geol. Prov: Silverwood province. Subdivided into four lithological packages; includes a subunit, Kelvin Falls Sill.||||||07-FEB-11
73063|Bald Hill Formation|68679|5|Briefly described|p445-447|Emsian|Emsian|Van Noord (1999). Silverwood Province. ~2450m thick. Considerable material was derived from older Silverwood Group.||Silverwood Group.||Unconformably overlies Connolly Volcanics. Is overlain by Ormoral Volcanics conformably and Bromley Hills Formation unconformably.|Basal polymictic conglomerate and breccia; middle unit mainly syn-depositional sills and cryptodomes (low-K tholeiitic basalt), some peperite, volcaniclastics, minor lava and limestone; upper turbidites and some chert with abundant slumping.|
73063|Bald Hill Formation|71628|5|Briefly described|p16: 4|||||Silverwood Group.||Is intruded by Cullendore Syenogranite.||
69498|Baldick Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Medium- to coarse-grained, even-grained biotite granite.|
69498|Baldick Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Medium- to coarse-grained, even-grained biotite granite.|
23353|Balfes Creek Granodiorite|22847|3|Fully described|p 49|Early Devonian|Late Silurian|||||||
23353|Balfes Creek Granodiorite|23422|5|Briefly described|p191|Middle Devonian|Silurian|||||||
23353|Balfes Creek Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 458. I-Type.||||||
23353|Balfes Creek Granodiorite|42633|5|Briefly described|Table 1 P8|||Reserved.||||||
23353|Balfes Creek Granodiorite|42750|2|Defined|p43|Early Devonian|Late Silurian|||||||
23353|Balfes Creek Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23353|Balfes Creek Granodiorite|43259|4|Described|Appendix 1,p49.|Early Devonian|Late Silurian|Rb-Sr age is 418+/-5 Ma.||||||
23353|Balfes Creek Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23353|Balfes Creek Granodiorite|62075|6|Mentioned|p15 Fig.7|Late Silurian|Late Silurian|Ravenswood batholith. Appears as Balfes Creek granodiorite.||||||
36156|Balfes Creek beds|23430|4|Described|p504 Table 14.5|Early Permian|Late Carboniferous|Also see p520. Overlain by Campaspe Formation.||||||21-AUG-08
36156|Balfes Creek beds|23505|5|Briefly described|Map legend|Permian|Late Carboniferous|||||||
36156|Balfes Creek beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Ellenvale and Wade beds; Insolvency Gully and Marshs Creek Formations; and Silver Valley Conglomerate, are all mapped under the symbol, CPs.||||||
36156|Balfes Creek beds|68731|6|Mentioned|p199|||Term used to describe a unit thought to represent the Boonderoo beds, occuring beyond the basin margin drilled at Balfes Creek.||||||
36156|Balfes Creek beds|72088|6|Mentioned|p94|||||||||
34128|Ballabay Complex|22630|5|Briefly described|p37|||||||||
34128|Ballabay Complex|22844|6|Mentioned|p37|||||||||
34128|Ballabay Complex|23049|3|Fully described|p63|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
34128|Ballabay Complex|23283|2|Defined|p27|Ordovician|Cambrian|||||||
34128|Ballabay Complex|23508|5|Briefly described|Map Legend|Permian|Ordovician|||||||
82290|Ballandean Monzogranite|71628|3|Fully described|p12: 1-2, 6-7, 13-14; p15: 33, 40, 82,97|Early Permian|Early Permian|See also 1-5,p15: 101-102; p19: 5-9. New name (this study); previously Ballandean Granite. Historically included within Stanthorpe Adamellite. Named after Ballandean Station. Forms a roughly 8 x 8 km intrusion at the W of Ballandean township. Crops out as sparse scattered boulders and pavements, and rare whalebacks. Two type locations have been proposed: GR 38238117 on Stanthorpe 1:100,000 sheet (Butler, 1974) and MGA 382406 6812031 (Donchak et al., 2007). Lithology, mineralogy and geochemistry detailed. Excluded from the new Sailor Jack Supersuite.|295 Ma (unpub. data in Rosenbaum et al., 2012)|Ballandean Suite.||Intrudes Texas beds. Is intruded by Sailor Jack, Severn River Monzogranites, Ruby Creek Leucogranite and Stanthorpe Complex. Is overlain unconformably by Wallangarra Volcanics.|White to grey, fine- to medium-grained, variably porphyritic hornblende-biotite monzogranite and biotite-hornblende-(clinopyroxene) granodiorite to monzogranite, and minor quartz monzonite. I-type.|
73886|Ballandean Suite|63748|5|Briefly described|p35, p43|||Of the Ballandean Supersuite. Includes the Ballandean Granite.||||||07-FEB-11
73886|Ballandean Suite|68679|5|Briefly described|p457-458|Permian|Permian|Northern New England Batholith. Geochemistry briefly described.|~295 Ma.|Stanthorpe Supersuite.|Ballandean Granite.|||
73886|Ballandean Suite|69639|6|Mentioned|p220|||||Ballandean Supersuite|Includes the Ballandean Granite.|||
73886|Ballandean Suite|71628|6|Mentioned|p12-6; p19-6||||||Ballandean Monzogranite.|||
73885|Ballandean Supersuite|63748|5|Briefly described|p36|||Includes the Ballandean and Sailor Jack Suite.||||||07-FEB-11
73885|Ballandean Supersuite|69639|5|Briefly described|p1, p44, p220|||New England Orogen.|||Includes the Sailor Jack Suite and the Ballandean Suite.|||
73885|Ballandean Supersuite|70876|5|Briefly described|p80|||Donchak et al (2013) incorporated this Supersuite into the Stanthorpe Supersuite; the authors of this volume however, note significant age ranges of the incorporated Supersuites and thus suggest this issue be revisited.||||||
73885|Ballandean Supersuite|71628|5|Briefly described|p12: 1, 8-12, 15; p19: 6|||Donchak et al. (2007). Modified in this study to form the Sailor Jack Supersuite (new name).|||Ballandean, Sailor Jack Suites.|||
27702|Ballara Quartzite|22623|6|Mentioned|p225,6||Proterozoic|||||||
27702|Ballara Quartzite|23079|6|Mentioned|p701||Mesoproterozoic|||||||
27702|Ballara Quartzite|23324|5|Briefly described|p468 Fig.1|||Metaquartzite.||||||07-FEB-07
27702|Ballara Quartzite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1755+/-3Ma. Said to be depositional age from dating of tuff. No information on where in the unit the tuff sits (base, top, mid?)||||||28-FEB-13
27702|Ballara Quartzite|23396|6|Mentioned|p422|||||||||
27702|Ballara Quartzite|23518|4|Described|p10|Proterozoic|Proterozoic|Of Mary Kathleen Group.  Geological Province: Eastern Fold Belt.||||||
27702|Ballara Quartzite|24197|6|Mentioned|p92|||Interbedded with felsic volcanics coeval with the intrusive Burstall Suite.||||||07-FEB-11
27702|Ballara Quartzite|24254|6|Mentioned|p22|||||||||
27702|Ballara Quartzite|24259|6|Mentioned|p108|||Geological Province: Mount Isa Block.||||||
27702|Ballara Quartzite|24308|5|Briefly described|p991|Paleoproterozoic|Paleoproterozoic|Geological Province: Eastern Fold Belt||||||07-NOV-08
27702|Ballara Quartzite|24432|4|Described|p562 Fig.2|Statherian|Statherian|Overlies Mitakoodi Quartzite. Overlain by Overhang Jaspilite. Age: 1756+/-3 Ma. Geological Province: Eastern Fold Belt.||||||
27702|Ballara Quartzite|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27702|Ballara Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mary Kathleen Group.  Underlies the Corella Formation.||||||25-AUG-04
27702|Ballara Quartzite|30531|3|Fully described|p15|||||||||
27702|Ballara Quartzite|30532|6|Mentioned|p113|||||||||
27702|Ballara Quartzite|30536|6|Mentioned|p100|||Stratigraphy||||||
27702|Ballara Quartzite|31704|6|Mentioned|p24|||Mineralization in Cloncurry||||||
27702|Ballara Quartzite|32660|5|Briefly described|Table 5|||||||||
27702|Ballara Quartzite|32770|5|Briefly described|p44|||Geological plan. See also p45.||||||15-MAR-07
27702|Ballara Quartzite|32959|6|Mentioned|Fig.21|||||||||
27702|Ballara Quartzite|33214|6|Mentioned|Fig.1|||||||||
27702|Ballara Quartzite|33900|5|Briefly described|p17|||Mention p15.||||||15-MAR-07
27702|Ballara Quartzite|35074|6|Mentioned|Fig.2|||||||||
27702|Ballara Quartzite|35116|6|Mentioned|Fig.2|||||||||
27702|Ballara Quartzite|35286|6|Mentioned|Fig.17|||||||||
27702|Ballara Quartzite|35470|6|Mentioned|p22|||||||||
27702|Ballara Quartzite|35932|6|Mentioned|p455|||||||||
27702|Ballara Quartzite|36052|6|Mentioned|p419|||See also Fig.2.||||||
27702|Ballara Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27702|Ballara Quartzite|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
27702|Ballara Quartzite|36963|6|Mentioned|p241|||||||||
27702|Ballara Quartzite|37568|4|Described|p83|||||||||
27702|Ballara Quartzite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27702|Ballara Quartzite|37862|6|Mentioned|p583|||||||||
27702|Ballara Quartzite|38234|6|Mentioned|p110|||See also Fig.2.||||||
27702|Ballara Quartzite|38235|6|Mentioned|p115|||||||||
27702|Ballara Quartzite|38276|6|Mentioned|Fig.1|||||||||
27702|Ballara Quartzite|38350|4|Described|p11|||||||||
27702|Ballara Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27702|Ballara Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27702|Ballara Quartzite|38833|6|Mentioned|p161|||||||||
27702|Ballara Quartzite|38834|6|Mentioned|p162|||||||||
27702|Ballara Quartzite|39445|6|Mentioned|p36|||Probably continuous with Quilalar Form. See also Table 2||||||
27702|Ballara Quartzite|39622|6|Mentioned|Fig.2|||||||||
27702|Ballara Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27702|Ballara Quartzite|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27702|Ballara Quartzite|39937|6|Mentioned|Fig.1|||||||||
27702|Ballara Quartzite|40221|6|Mentioned|p11|||||||||
27702|Ballara Quartzite|40623|5|Briefly described|p95|||||||||
27702|Ballara Quartzite|40648|3|Fully described|p9|||||||||
27702|Ballara Quartzite|40840|6|Mentioned|Map legend|||||||||
27702|Ballara Quartzite|40984|4|Described|p389|||||||||
27702|Ballara Quartzite|41069|6|Mentioned|p452|||||||||
27702|Ballara Quartzite|41150|5|Briefly described|Fig.1|||||||||
27702|Ballara Quartzite|41744|6|Mentioned|p406|||||||||
27702|Ballara Quartzite|41761|6|Mentioned|Fig.1|||||||||
27702|Ballara Quartzite|41791|6|Mentioned|p266|||||||||
27702|Ballara Quartzite|41978|6|Mentioned|p490|||||||||
27702|Ballara Quartzite|41979|6|Mentioned|p538|||||||||
27702|Ballara Quartzite|42201|6|Mentioned|p292|||||||||
27702|Ballara Quartzite|42234|5|Briefly described|p1055|||||||||
27702|Ballara Quartzite|42365|5|Briefly described|Fig.1 P256|||Also Fig.3, Fig.21||||||
27702|Ballara Quartzite|42565|4|Described|Table 1 P5, P2|||||||||
27702|Ballara Quartzite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Sandstone, arkose, conglomerate.||||||09-FEB-09
27702|Ballara Quartzite|42781|5|Briefly described|Fig.3 P428|||see also Fig.1 p426.||||||15-MAR-07
27702|Ballara Quartzite|42818|5|Briefly described|Fig.2 P205|||||||||
27702|Ballara Quartzite|42858|5|Briefly described|p671|||||||||
27702|Ballara Quartzite|42859|5|Briefly described|p675|||||||||
27702|Ballara Quartzite|42879|6|Mentioned|p213|||||||||
27702|Ballara Quartzite|43643|5|Briefly described|p612|||||||||
27702|Ballara Quartzite|44275|14|Not recorded|Map Legend|||||||||
27702|Ballara Quartzite|44989|2|Defined|Not recorded|||||||||
27702|Ballara Quartzite|45136|3|Fully described|p24|||||||||
27702|Ballara Quartzite|45161|6|Mentioned|p16|||||||||
27702|Ballara Quartzite|45166|4|Described|p20|||||||||
27702|Ballara Quartzite|45287|14|Not recorded|p.225,226|||||||||
27702|Ballara Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
27702|Ballara Quartzite|46843|6|Mentioned|Fig.2|||||||||
27702|Ballara Quartzite|46960|6|Mentioned|p215|||||||||
27702|Ballara Quartzite|46962|4|Described|Table 1|||See also Fig.3.||||||
27702|Ballara Quartzite|46995|5|Briefly described|p268|||||||||
27702|Ballara Quartzite|46996|6|Mentioned|p273|||||||||
27702|Ballara Quartzite|47083|6|Mentioned|p10|||Of Mary Kathleen Group.||||||
27702|Ballara Quartzite|49009|6|Mentioned|p44|||||||||
27702|Ballara Quartzite|49041|6|Mentioned|Table 4|||||||||
27702|Ballara Quartzite|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Mainly quartzite and feldspathic sandstones, commonly metamorphosed to quartzite.  Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.  ||||||
27702|Ballara Quartzite|50332|5|Briefly described|p16, p18|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Consists of quartz and feldspathic sandstones that are commonly metamorphosed to quartzite.||||||07-FEB-11
27702|Ballara Quartzite|50536|5|Briefly described|p1.1, 5.2, 6.1|||Geological Province: Mount Isa Inlier. Age: 1755 +/- 3Ma (Shrimp).||||||
27702|Ballara Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Meta-arenite.||||||
27702|Ballara Quartzite|61922|5|Briefly described|p8, p9 Fig. 3, p17 Fig. 9|Paleoproterozoic|Paleoproterozoic|Tog. with Mitakoodi Quartzite and part Quilalar Quartzite forms marker horizon within cover seq. 2. Overlies Argylla Formation unconformably. Age:ca1755Ma. Geol. Prov: Mount Isa Inlier/Eastern Fold Belt. ||||||07-NOV-08
27702|Ballara Quartzite|61925|5|Briefly described|p57 Fig. 2, p64|||Of the Malbon Group. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||15-MAR-07
27702|Ballara Quartzite|61926|5|Briefly described|p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Malbon Group. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
27702|Ballara Quartzite|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Mary Kathleen Group. Age: 1755+/-3Ma. ||||||07-NOV-08
27702|Ballara Quartzite|61933|6|Mentioned|p177|||||||||
27702|Ballara Quartzite|61936|5|Briefly described|p195 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1755Ma. Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
27702|Ballara Quartzite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Quilalar Supersequence spanning the interval ~1755-1740Ma (Mary Kathleen zone). Geological Province: Mount Isa Inlier.||||||07-NOV-08
27702|Ballara Quartzite|63023|6|Mentioned|p1034|Paleoproterozoic|Paleoproterozoic|Age: 1755+/-3Ma. In the Mary Kathleen region of the Eastern Fold Belt.||||||07-NOV-08
27702|Ballara Quartzite|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Appears in Fig.2 as Ballara (Mitakoodi) Quartzite. |Between c.1840 and 1800 Ma.||||Sandstone, siltstone, greywacke, basalt.|
27702|Ballara Quartzite|63866|4|Described|p60|Statherian|Statherian|Leichhardt Superbasin. Numeric age is derived from Page (OZCHRON).|1755 +/- 3 Ma (Stratigraphic age of protolith)|||Overlain by the Corella Formation. Intruded by the Wonga Suite.|Quartzite, micaceous quartzite and tuffaceous quartzite.|
27702|Ballara Quartzite|64248|5|Briefly described|p32-33, p36, p38 Fig.5, p40-41, p46|Statherian|Statherian|Foster and Austin (2008) proposed this unit's age is equivalent with Mitakoodi Quartzite. Shown as BM Quartzite, for Ballara and Mitakoodi quartzites (p33 Fig.1, p41 Tb. 2)|1755 +/- 3 Ma.|||||11-DEC-17
27702|Ballara Quartzite|64250|5|Briefly described|p7-8, p10-12, p15, p18, p22-23, p26|||80-1250m thick going westwards. Given geochronological and lithological similarities, the two units (Ballara-Mitakoodi Quartzite) are here treated as a single fluvial, near-shore beach, and shallow marine sequence, with this (hopefully temporary) name, and referred to in figure as BM Quartzite (Fig.2, Fig.8).|1755 +/- 3 Ma|Mary Kathleen Group||Equivalent to Mitakoodi Quartzite.  Overlain by Corella Formation. Overlies Argylla Formation (unconformably).|Sandstone, quartzite; minor metabasalt and felsic tuff.|
27702|Ballara Quartzite|64744|6|Mentioned|p353 Fig.4, p357 Fig.6.|Statherian|Statherian|Mount Isa Basin.|||||Metaquartzite.|
27702|Ballara Quartzite|65387|6|Mentioned|p60|||||||Unconformably overlies Argylla suite (or may be intruded by it?).||
27702|Ballara Quartzite|65396|5|Briefly described|p7, p15-17, p77, p82,p84, p169, p173-175|Statherian|Statherian|See also p177-178, p180-184, p187, p190, p194, p196, p201-202, p217, p241, p439. With the Mitakoodi Quartzite forms a single regionally extensive sequence. Up to 1250m thick; thins eastward to 80m. Leichhardt Superbasin. Eastern succession, Cover Sequence 3. Kalkadoon-Leichhardt Belt, Mary Kathleen Fold Belt. Fluvial, near-shore beach, and shallow-marine sequence. Hosts numeous Cu+/- Au occurrences.|1755 +/- 3 Ma - 1762 +/- 3 Ma|Mary Kathleen Group||Unconformably overlies Argylla Formation, overlies Tewinga Group. Conformably overlain by Corella Formation. (Possibly) correlated with Mitakoodi Quartzite, Makbat Sandstone, Stanbroke Sandstone.|Predominantly sandstone and quartzite with minor mafic volcanics and felsic tuff.|03-APR-17
27702|Ballara Quartzite|65505|5|Briefly described|965-66, 974, 979-981, Fig 1-3,6|Proterozoic|Proterozoic|Overlies the Argylla Formation unconformably. Conglomerate, arkose, white quartzite. Grey coloured, thinly laminated, fine grained. Age: 1767 +/- 4 Ma.||||||
27702|Ballara Quartzite|65755|6|Mentioned|p3 Fig.1|||Presented in figure legend as Ballara-Mitakoodi Quartzite||||||
27702|Ballara Quartzite|67323|5|Briefly described|p11, p15-16, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Marks the end of extension of the Leichhardt Superbasin. Western Mary Kathleen Domain. Usually thin (<200m); thickens locally to >1500m. Is intruded by Wonga Suite. An MDA of 1767 +/- 4 Ma (Neumann et al., 2009) is given.|1755 +/- 3 Ma (Page, 1988).|||Unconformably overlies Argylla Formation. Is overlain by Corella Formation. Equivalent to Quilalar Formation, probably Mitakoodi Quartzite (at least partly), and ?upper Boomarra Metamorphics.|Quartzite, micaceous quartzite, minor pebble beds.|
27702|Ballara Quartzite|67539|5|Briefly described|p10, p11|||Commonly contains a basal conglomerate with clasts of the underlying Argylla Formation. Generally <200m thick. See also Ballara Formation, same pages.||||Underlain by the Argylla Formation.||
27702|Ballara Quartzite|68021|6|Mentioned|p135 fig 4, p136|Statherian|Statherian|Eastern Succession.||||Overlain by Corella Formation, intruded by Wonga Granite, Burstal Granite. Lateral equivalent to Quilalar Supersequence.||
27702|Ballara Quartzite|68542|6|Mentioned|p12, p20 fig 6|||||Mary Kathleen Group||Unconformably overlies Argylla Formation, overlain by Corella Formation|Calcareous rock and arkosic sandstone, Quartzite.|
27702|Ballara Quartzite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Corella Formation under the symbol, -Pk.||||||
27702|Ballara Quartzite|68575|4|Described|p1-2, p6-7, p63, p75-81, p124, p126,p134|||Mount Isa Region. Sampled rock originally mapped (Wilson and Grimes, 1986) as Argylla Formation, overlying Magna Lynn Metabasalt, and underlying Ballara Quartzite and Corella Formation. Thickness ranges from zero to about 1000m. Age of an intercalated feldspar-phyric rhyolite. A tuffaceous quartzite within this unit was dated at 1755 +/- 3 Ma (Page, 1998), and a previous (Neumann et al., 2009) detrital zircon maximum deposition age was determined at 1767 +/- 4 Ma for the upper part of the unit. The lower part may be an equivalent of the Myally Subgroup. Whole rock Sm-Nd isotopic data and age (1768 Ma).|1769 +/- 6 Ma.|||Is overlain by Corella Formation.|Includes intercalated porphyritic rhyolite.|17-JAN-17
27702|Ballara Quartzite|68576|5|Briefly described|Q-2: p12-13, p20||||1755 Ma.|Basal Mary Kathleen Group.||Unconformably overlies Argylla Formation. Is overlain by Corella Formation.|Includes a basal calcareous arkose facies.|
27702|Ballara Quartzite|68732|5|Briefly described|p161, p162, p165-167, p169, p171|Statherian|Statherian|Contains flat rhythmites. Of the Quilalar Supersequence. Maximum depositional sedimentary age.|1755 +/- 3 Ma||||Includes fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones; very fine-grained arkosic sandstones. Also sandstone-siltstone-shale laminae and thin beds (rhythmites).|30-NOV-17
27702|Ballara Quartzite|69056|5|Briefly described|p2-3, p5, p53|Statherian|Statherian|See also Time-Space plot sheet, Reference images sheet. Mary Kathleen Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Corella Formation. Age from a tuff layer within the sequence. Also maximum depositional age of 1767 +/- 4 Ma (Neumann et al., 2009).|1755 +/- 3 Ma (Page, 1988).|||Overlies Argylla Formation and Boomarra Metamorphics. Is overlain by Corella Formation. Equivalent to Mitakoodi Quartzite.||
27702|Ballara Quartzite|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Eastern Fold Belt.|1755 +/- 3 Ma|Mary Kathleen Group||Overlies Mitakoodi Quartzite, overlain by Corella Formation, Mount Albert Group||09-FEB-18
27702|Ballara Quartzite|69591|4|Described|p29, p33-35, p57, p105|Paleoproterozoic|Paleoproterozoic|Williams et al. (1989). Mary Kathleen Domain, Leichhardt Superbasin, Mount Isa Province. Part of the Quilalar Supersequence. Near shore/beach deposits. Usually <200m thick; thickens to >1500m SE of Dobbyn. Age from tuff.|1755 +/- 3 Ma; Page (1998).|Mary Kathleen Group.||Unconformably overlies Argylla Formation. Is overlain by Corella Formation.|Predominantly quartzose sandstone: quartzite, micaceous quartzite, minor pebble beds.|
27702|Ballara Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group.||Is overlain by Corella Formation.|Quartzite, locally micaceous; minor conglomerate. (Separately mapped) very coarse-grained, feldspathic sandstone to granule conglomerate; local pebble to boulder conglomerate.|
27702|Ballara Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group.||Is overlain by Corella Formation.|Quartzite, locally micaceous; minor conglomerate. (Separately mapped) very coarse-grained, feldspathic sandstone to granule conglomerate; local pebble to boulder conglomerate.|
27702|Ballara Quartzite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group.|||Quartzite, locally micaceous; minor conglomerate. (Separately mapped) strongly lineated mylonitic quartzite.|
27702|Ballara Quartzite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group.|||Quartzite, locally micaceous; minor conglomerate. (Separately mapped) strongly lineated mylonitic quartzite.|
27702|Ballara Quartzite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group.||Is overlain by Corella Formation.|Quartzite, locally micaceous; minor conglomerate.|
27702|Ballara Quartzite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mary Kathleen Group|||Quartzite, locally micaceous; minor conglomerate.|
27702|Ballara Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1769+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
27702|Ballara Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Ages given as U-Pb zircon sedimentary depositional ages.|1769 +/- 6 Ma, 1755 +/- 3 Ma|||Shown as partially overlying Argylla Formation.||
27702|Ballara Quartzite|72596|6|Mentioned|p1, p4, p23, p63|Statherian|Statherian|Geochronologic constraint is a crystallisation age of metarhyolites from Magee et al. (2012).|1769 +/- 6 Ma|||Partly overlain conformably by Corella Formation in the north.|Includes metarhyolite.|
27702|Ballara Quartzite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||Mary Kathleen Group||Underlies Corella Formation.|Quartzite, locally micaceous quartzite; minor pebble beds.|
27702|Ballara Quartzite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||Mary Kathleen Group||Underlies Corella Formation.|Quartzite, locally micaceous quartzite; minor pebble beds.|
27702|Ballara Quartzite|72799|6|Mentioned|p4|||||||||
27702|Ballara Quartzite|72889|6|Mentioned|p6 Fig.i.|||||||||
27702|Ballara Quartzite|73042|6|Mentioned|p4|Statherian|Statherian|Mount Isa Province, Leichhardt Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1755 +/- 3 Ma, 1769 +/- 6 Ma (see Fig.1.2)|||||
27702|Ballara Quartzite|73137|5|Briefly described|p2, p5-6, p13, p15-18|Statherian|Statherian|Geochron is a maximum depositional age. Sampled locality was previously mapped as Corella Formation but was herein reassigned based on new geochronolgy. Age is closely comparable to that from felsic volcanics of the Argylla Formation, which raises questions about its true attribution [see article]. Locally exhibits planar and cross bedding. [See article for Ballara Quartzite sample field description, petrographic description and detailed geochronology].|1776 +/- 4 Ma|||Conformably overlain by Corella Formation. Intruded by Mount Maggie Granite.|Includes quartzose metasandstone.|
27702|Ballara Quartzite|73413|6|Mentioned|p3, p23, App.1|Statherian|Statherian|Mount Isa Inlier. U-Pb SHRIMP age of 1780 +/- 4 Ma reported by Neumann et al. (2006) and 1767 +/- 4 Ma by Neumann et al. (2009).|ca. 1755 Ma|||Underlain by Argylla Formation.||
27702|Ballara Quartzite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Kalkadoon-Leichhardt and Mary Kathleen Domains.|1767+/-4 Ma MDA, 1755+/-3 Ma age of volcanic rock||||Siliciclastics, minor mafic extrusives.|
27702|Ballara Quartzite|73529|5|Briefly described|p4, p6 Fig.3|Statherian|Statherian|Represents transition to a nearshore depositional environment.|1767+/-4 Ma (Neumann et al., 2009)|||Overlies Argylla Formation|Characterised by quartzite, micaceous quartzite and minor pebble beds.|
27702|Ballara Quartzite|73553|5|Briefly described|p1, p7, p8 Fig.1.2.3, p23, p27, p68-70,|Statherian|Statherian|Mary Kathleen Domain. Multiple maximum depositional ages provided. See also p74, p95, p144 Fig.5.4.6.|1776+/-4 Ma to 1767+/-4 Ma, 1755 Ma MDA|Mary Kathleen Group||Unconformably overlies Argylla Formation, underlies Corella Formation||03-FEB-23
36238|Ballast Creek Dacite|23423|5|Briefly described|p309 Table 7.3||Late Carboniferous|Of Claret Creek Volcanics.||||||09-SEP-08
36238|Ballast Creek Dacite|23502|5|Briefly described|Map Legend||Late Carboniferous|In the Claret Creek Ring Complex; Claret Creek Supersuite.||||||09-SEP-08
36238|Ballast Creek Dacite|23624|4|Described|p25|||Of the Claret Creek Supersuite.||||||02-JUN-09
36238|Ballast Creek Dacite|60425|4|Described|p50 Tb. 3, p282-3 Appdx. |Late Carboniferous|Late Carboniferous|Of Claret Creek Volcanics (Claret Creek Supersuite). Age: 300+/-6Ma (Rb-Sr). Pink to pinkish grey, and grey, lithics-poor to -rich, welded dacitic ignimbrite; intrusive dacite, rhyodacite and breccia. I-type.||||||07-FEB-11
36238|Ballast Creek Dacite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Pale grey, intrusive dacite, rhyodacite and breccia with clasts up to ~30 cm across.|
36238|Ballast Creek Dacite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Pale grey, intrusive dacite, rhyodacite and breccia with clasts up to ~30 cm across.|
29619|Ballogie Suite|43005|5|Briefly described|p217|||||||||
23356|Bally Knob Volcanics|23074|5|Briefly described|p737 (Fig 1)|Carboniferous|Carboniferous|||||||
23356|Bally Knob Volcanics|23291|4|Described|p43, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||
23356|Bally Knob Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V38. I-Type.||||||
23356|Bally Knob Volcanics|23619|4|Described|p30 table 1||Carboniferous|Also see p9. Divided into 4 unnamed units. McBride Basalt Group - unconformable. Balcooma Metavolcanics, Eland Metavolcanics + Dido Tonalite - unconformable contact for all 3 units.||||||
23356|Bally Knob Volcanics|41675|2|Defined|p73|Carboniferous||||||||
23356|Bally Knob Volcanics|42054|6|Mentioned|p272|||||||||
23356|Bally Knob Volcanics|42279|4|Described|p22|||See also Fig.3||||||
23356|Bally Knob Volcanics|42692|5|Briefly described|map legend|Carboniferous||||||||
23356|Bally Knob Volcanics|42933|5|Briefly described|p220|||||||||
23356|Bally Knob Volcanics|43113|4|Described|Table 1,p18.||Carboniferous|||||||
23356|Bally Knob Volcanics|43253|5|Briefly described|map legend||Carboniferous|||||||
23356|Bally Knob Volcanics|43259|4|Described|Appendix 1,p4.||Carboniferous|||||||
23356|Bally Knob Volcanics|50202|5|Briefly described|Map legend|Early Permian|Carboniferous|Porphyritic flow-banded rhyolite, rhyolitic ignimbrite, aphyric dacite, dacitic volcaniclastic rocks.||||||
23356|Bally Knob Volcanics|68344|5|Briefly described|Map legend.|Early Permian|Carboniferous|Four facies are mapped separately. Parts of this unit have high K, Th and U radiometric responses.|||||Purple, crystal-rich dacitic volcaniclastic rocks including ignimbrite; green aphyric dacite; pink to brown, crystal-poor rhyolitic ignimbrite; pink to brown, sparsely porphyritic, flow-banded rhyolite.|
23356|Bally Knob Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
23356|Bally Knob Volcanics|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned.|||||Rhyolitic ignimbrites, rhyolitic-dacitic lavas and tuff; mostly minor to rare basalt and andesite.|
27637|Ballynure Rhyolite|23032|5|Briefly described|p42,43||Carboniferous|||||||
27637|Ballynure Rhyolite|23291|5|Briefly described|p91 Fig. 3.9|Carboniferous|Carboniferous|Parent: Butlers Volcanic Group. Age: About 330Ma. Thickness: Up to 120m. Geological Province: Georgetown Region.||||||18-JUN-15
27637|Ballynure Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V35. I-Type.||||||
27637|Ballynure Rhyolite|23619|5|Briefly described|p32 Table 1|||Overlying Unit Edmonds Creek Rhyolite||||||
27637|Ballynure Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27637|Ballynure Rhyolite|40542|6|Mentioned|p97|||||||||
27637|Ballynure Rhyolite|43113|6|Mentioned|Table 1 p19|||||||||
27637|Ballynure Rhyolite|43259|4|Described|Appendix 1,p4.||Carboniferous|Of Butlers Volcanic Group.||||||12-JUN-08
27637|Ballynure Rhyolite|43286|5|Briefly described|Map Legend||Carboniferous|of Butlers Volcanic Group.||||||
27637|Ballynure Rhyolite|43740|4|Described|p24|||||||||
27637|Ballynure Rhyolite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Butlers Volcanic Group.||||||
27637|Ballynure Rhyolite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of Butlers Volcanic Group.||||||
27637|Ballynure Rhyolite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province.||Unit in Butlers Volcanic Group.|||Purple crystal-rich rhyolitic ignimbrite; pink, green or purple, crystal-rich and very crystal-rich rhyolitic ignimbrite with moderately abundant lithic clasts.|
27637|Ballynure Rhyolite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure.||Of the Butlers Volcanic Group.||Conformably overlain by the Edmonds Creek Rhyolite.|Pink, green or purple, crystal-rich and very crystal-rich rhyolitic ignimbrite with moderately abundant lithic clasts; purple, crystal-rich rhyolitic ignimbrite.|
30124|Banana Microgranite|22847|3|Fully described|p 58|Permian|Carboniferous|||||||
30124|Banana Microgranite|23422|5|Briefly described|p218 Table 6.12|||Of Bogie Suite.||||||
30124|Banana Microgranite|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30124|Banana Microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 187. I-Type.||||||
30124|Banana Microgranite|43093|4|Described|Appendix 1|Permian|Carboniferous|Invalid name. Banana Formation already in use in Qld.||||||
30124|Banana Microgranite|43259|4|Described|Appendix 1,p28.|Permian|Carboniferous|||||||
30124|Banana Microgranite|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30124|Banana Microgranite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Bogie Suite.||||
27325|Barfield Formation|13516|5|Briefly described|p145 fig 3|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5004||||||
27325|Barfield Formation|22973|5|Briefly described|p10|Late Permian|Late Permian|||||||
27325|Barfield Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
27325|Barfield Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
27325|Barfield Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
27325|Barfield Formation|23037|5|Briefly described|p64,5,66||Permian|Equivalent to Back Creek Group, contains Four Mile Mudstone, Cottenham Sandstone and Station Mudstone Members. Max. thickness 700 m.||||||22-MAR-12
27325|Barfield Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
27325|Barfield Formation|24491|5|Briefly described|p20|||Geological Province: Bowen Basin.||||||
27325|Barfield Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbr].  Mudstone, siltstone, lithic and feldspathic sandstone, minor conglomerate.||||||
27325|Barfield Formation|29436|6|Mentioned|p317||Permian|||||||
27325|Barfield Formation|29964|6|Mentioned|p5|||||||||
27325|Barfield Formation|30141|5|Briefly described|p134|||||||||
27325|Barfield Formation|30449|6|Mentioned|p4|||Brachiopods. See also P6,8,14,21||||||
27325|Barfield Formation|30450|6|Mentioned|Table 1|||Permian age.Southeast Bowen Basin||||||
27325|Barfield Formation|30451|3|Fully described|p54|||See also p55,56.||||||16-NOV-15
27325|Barfield Formation|30546|6|Mentioned|p107|||Upper Permian age. Correlation.See also P114,fauna||||||
27325|Barfield Formation|30743|6|Mentioned|p24|||Geological map||||||
27325|Barfield Formation|30916|6|Mentioned|p98|||||||||
27325|Barfield Formation|31079|6|Mentioned|Fig. 6|||||||||
27325|Barfield Formation|32577|6|Mentioned|p23|||Unit of Blenheim Sub Gp.||||||
27325|Barfield Formation|33711|6|Mentioned|Table 3|||||||||
27325|Barfield Formation|33745|6|Mentioned|p204|||||||||
27325|Barfield Formation|33774|3|Fully described|p35|||Map||||||
27325|Barfield Formation|34132|6|Mentioned|p2|||Upper Permian||||||
27325|Barfield Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
27325|Barfield Formation|35284|6|Mentioned|Fig.1|||||||||
27325|Barfield Formation|35426|3|Fully described|p656|||||||||
27325|Barfield Formation|35845|6|Mentioned|Fig.36|||||||||
27325|Barfield Formation|35873|6|Mentioned|Fig.38|||||||||
27325|Barfield Formation|36241|6|Mentioned|p130|||||||||
27325|Barfield Formation|36243|6|Mentioned|Table 4A|||||||||
27325|Barfield Formation|36333|6|Mentioned|Map legend|Late Permian|Late Permian|Of the Back Creek Group.||||||15-JUL-04
27325|Barfield Formation|36739|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|36925|6|Mentioned|p179|||||||||
27325|Barfield Formation|37075|5|Briefly described|Table 1|||||||||
27325|Barfield Formation|37756|6|Mentioned|p73|||||||||
27325|Barfield Formation|37858|6|Mentioned|p82|||||||||
27325|Barfield Formation|38204|4|Described|p75|||||||||
27325|Barfield Formation|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27325|Barfield Formation|39212|5|Briefly described|p12|||||||||
27325|Barfield Formation|39252|6|Mentioned|Fig.13|||||||||
27325|Barfield Formation|39261|6|Mentioned|Fig.6|||||||||
27325|Barfield Formation|39262|6|Mentioned|p126|||||||||
27325|Barfield Formation|39267|6|Mentioned|p238|||See also P240||||||
27325|Barfield Formation|39445|5|Briefly described|Table 8|||||||||
27325|Barfield Formation|39943|6|Mentioned|Table 6A|||||||||
27325|Barfield Formation|40091|6|Mentioned|p72|||||||||
27325|Barfield Formation|40093|4|Described|p32|||||||||
27325|Barfield Formation|40539|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|41246|6|Mentioned|Map legend|Permian||||||||
27325|Barfield Formation|41546|6|Mentioned|Fig.2|||||||||
27325|Barfield Formation|41666|5|Briefly described|p3|||||||||
27325|Barfield Formation|41809|6|Mentioned|p64|||||||||
27325|Barfield Formation|42249|6|Mentioned|p22|||||||||
27325|Barfield Formation|42250|6|Mentioned|Fig.4 P31|||||||||
27325|Barfield Formation|42641|6|Mentioned|Fig.3 P110|||||||||
27325|Barfield Formation|42994|6|Mentioned|p149|||||||||
27325|Barfield Formation|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
27325|Barfield Formation|43017|5|Briefly described|Fig.3,p375|||||||||
27325|Barfield Formation|43050|5|Briefly described|p4|||||||||
27325|Barfield Formation|43185|6|Mentioned|6||Late Permian|||||||
27325|Barfield Formation|43460|14|Not recorded|p100|||||||||
27325|Barfield Formation|43471|14|Not recorded|p247,248|||Megadesmus, Astartila||||||
27325|Barfield Formation|43474|14|Not recorded|p66,74,52,104|||Permian fossils||||||
27325|Barfield Formation|43475|14|Not recorded|p553,555|||||||||
27325|Barfield Formation|43585|6|Mentioned|p15||Late Permian|||||||
27325|Barfield Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
27325|Barfield Formation|43894|14|Not recorded|p791|||||||||
27325|Barfield Formation|43987|14|Not recorded|p267,270|||||||||
27325|Barfield Formation|43994|14|Not recorded|Map Legend|||||||||
27325|Barfield Formation|44118|14|Not recorded|Map Legend||Late Permian|||||||
27325|Barfield Formation|44169|2|Defined|Tb.1,p8,map||Late Permian|||||||
27325|Barfield Formation|44170|4|Described|Tb.1,8,9,11||Late Permian|||||||
27325|Barfield Formation|44218|14|Not recorded|p17,19||Kazanian|||||||
27325|Barfield Formation|44243|14|Not recorded|p649,map||Late Permian|||||||
27325|Barfield Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
27325|Barfield Formation|44381|14|Not recorded|p6|||Equivalent to Orange Creek, Acacia and Passion Hill Formations and to Four Mile Mudstone, Cottenham Sandstone and Station Mudstone.||||||
27325|Barfield Formation|44390|14|Not recorded|p15|||||||||
27325|Barfield Formation|44424|14|Not recorded|p293-301|||Passes laterally into Boomer Formation.||||||
27325|Barfield Formation|44426|14|Not recorded|p11|||||||||
27325|Barfield Formation|44427|14|Not recorded|p159,160,162-165|||Theodore-Banana area.||||||
27325|Barfield Formation|44490|14|Not recorded|p46,48|||Fossils.||||||
27325|Barfield Formation|44514|2|Defined|p27,30||Permian|Conformably overlies Oxtrack Formation. Conformably overlain by Orange Creek Formation. Basal formation of Back Creek Group. (Middle Permian).||||||20-MAY-08
27325|Barfield Formation|44571|2|Defined|p205-206,Fig.28|||||||||
27325|Barfield Formation|44640|14|Not recorded|p30|||||||||
27325|Barfield Formation|44857|14|Not recorded|p96-98||Permian|||||||
27325|Barfield Formation|44859|14|Not recorded|p67,72||Permian|Gastropods. Strotostoma, sp.nov.||||||
27325|Barfield Formation|45006|14|Not recorded|Tb.1,p5,6,97,103,140|||p144||||||
27325|Barfield Formation|45031|14|Not recorded|p9,Fig.3||Permian|||||||
27325|Barfield Formation|45071|3|Fully described|Table 10|||See also p54.||||||16-NOV-15
27325|Barfield Formation|46949|6|Mentioned|Fig.3|||||||||
27325|Barfield Formation|48898|6|Mentioned|p25|||Back Creek Group||||||
27325|Barfield Formation|48900|6|Mentioned|p84|||Table opposite.||||||
27325|Barfield Formation|48919|4|Described|p22|||See also P23-26||||||
27325|Barfield Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Back Creek Group.  Includes Four Mile Mudstone, Cottenham Sandstone, and Station Mudstone Members.||||||17-MAY-04
27325|Barfield Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Back Creek Group. Mudstone, siltstone, lithic and feldspathic sandstone and minor conglomerate.||||||
27325|Barfield Formation|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Back Creek Group.||||||27-MAY-04
27325|Barfield Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
27325|Barfield Formation|60282|5|Briefly described|p7|||Mudstone and some lithic sandstone. Passes laterally into undivided rocks of Back Creek Group.||||||20-MAY-08
27325|Barfield Formation|60330|5|Briefly described|p259|Late Permian|Late Permian|Geological Province: Bowen Basin||||||
27325|Barfield Formation|61076|5|Briefly described|p188 Fig. 2|Late Permian|Late Permian|Age: >260Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
27325|Barfield Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
27325|Barfield Formation|61778|5|Briefly described|p239||Late Permian|Geological Province: Bowen Basin.||||||07-FEB-11
27325|Barfield Formation|61782|5|Briefly described|p280|||Of Blenheim Subgroup. Contains tuffs and andesite.||||||
27325|Barfield Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
27325|Barfield Formation|63773|6|Mentioned|p1059|||||||||
27325|Barfield Formation|64856|3|Fully described|p42, p49, p52-53, p55 Fig.7, p66, p102|Late Permian|Late Permian|Derrington et al. (1959). Bowen Basin. Mudstones and siltstones with lesser sandstones, tuffs, conglomerates. Unconformably overlies Camboon Volcanics or Buffel Formation. Is overlain by Flat Top Formation. Age from palynoflora (formerly considered APP33, now APP5). Max thickness 714m.| | ||||28-NOV-17
27325|Barfield Formation|64857|5|Briefly described|p118-119, p113 Fig.3|Late Permian|Late Permian|Taroom Trough, Bowen Basin. Marine mudstones overlying the Oxtrack Formation.||||||
27325|Barfield Formation|64858|5|Briefly described|p181, p180 Fig.2, p182 Fig.3, p191|Late Permian|Late Permian|Bowen Basin. Includes coals.||||||30-NOV-09
27325|Barfield Formation|64859|6|Mentioned|p196, 225|Permian|Permian|Gas source rocks.||||||
27325|Barfield Formation|65112|5|Briefly described|p313; p316; p317; 321; Fig 4 p314.|Triassic|Late Permian|Post-extension sequences of the Taroom Trough. Interpreted as turbidite facies.||||Overlies the Oxtrack Formation; underlies Flat Top Formation.|Contains intervals that include breccia, diamictite and conglomerate that interrupted thin marine strata.|22-MAR-12
27325|Barfield Formation|65113|5|Briefly described|p349, Fig 4 p340|Late Permian|Late Permian|Taroom Trough. Deposited in a passive thermal subsidence phase. Fine grained deep water turbidites.Overlies Oxtrack Formation, underlies Flat Top Formation.||||||
27325|Barfield Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
27325|Barfield Formation|65115|5|Briefly described|p413, 415, Fig 2 p403|Kazanian|Ufimian|Underlies the  Flat Top Formation, Overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin. Part of Supersequence D. Includes mud and thin interbeds of feldspathic sandstone, in places calcareous.||||||
27325|Barfield Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|?Underlies the Flat Top Formation, Overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|?Underlies the Flat Top Formation, overlies the Oxtrack Formation in the Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|65119|6|Mentioned|Fig 4-6, Fig 9-10|||Present in the Cockatoo Creek 1 and Burunga 1 Wells.||||||
27325|Barfield Formation|65388|4|Described|p168-170, p161, 163, 166, 437, 439, 447|Roadian|Kungurian|Of Derrington & others (1959). Back Creek Group, Bowen Basin. Massive mudstone and subordinate siltstone, sandstone, tuff and conglomeratic mudstone and limestone sequence, dominantly marine,  conformably overlying the Oxtrack Formation in the Banana and Cracow areas, or disconformably overlying Buffel Formation, Camboon Volcanics. Conformably overlain by the Flat Top Formation. Correlated with Moah Creek beds. Age from marine fossils and palynoflora - Ufimian - Kazanian. Fossils correlated with Ingelara and lower Peawaddy Formations. Generally poor exposure. Minor tuff in upper part of Fmn.||||||16-NOV-15
27325|Barfield Formation|66615|6|Mentioned|p2 Fig.1, p9|||Southern Taroom Trough, Bowen Basin.||||||
27325|Barfield Formation|67402|6|Mentioned|p21, p45|Capitanian|Capitanian|Bowen Basin. ||||Overlain by the Burunga Formation. Overlies the Oxtrack Formation.||
27325|Barfield Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Flat Top Formation. Underlain by Oxtrack Formation.||
27325|Barfield Formation|68679|4|Described|p350, p353, p378, p380-382, p419|Permian|Permian|Derrington et al. (1959). SE Bowen Basin. 900m thick. Offshore marine with local turbidite fan deposits. Mentioned as having the same fossil species as, and thus establishing the age of, the Warminster Formation (Yarrol Province).||Back Creek Group.|Cottenham Sandstone Member.|Overlies Oxtrack Formation. Is overlain by Flat Top Formation. Correlates with Muggleton Formation. Is intruded by The Pride Gabbro.|Mudstone, siltstone and tuff; conglomerate and sandstone occur locally; marine fossils.|
27325|Barfield Formation|73450|6|Mentioned|p55|||Bowen Basin.||||||
27325|Barfield Formation|73570|6|Mentioned|p916|Late Permian|Late Permian|||||||
27325|Barfield Formation|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Taroom Trough, Eastern Bowen Basin.||||Overlies Moah Creek Beds. Is overlain by Flat Top Formation.||
69494|Barkers Basalt|68336|5|Briefly described|Map legend.|Quaternary|Quaternary|Nulla Basalt Province.|||||Olivine basalt.|
69494|Barkers Basalt|68338|5|Briefly described|Map legend.|Quaternary|Quaternary|Chudleigh Province.|0.26 Ma.||||Olivine basalt, scoria, volcanic cone or vent.|
69494|Barkers Basalt|68341|5|Briefly described|Map legend.|Quaternary|Quaternary|Nulla Basalt Province.|||||Olivine basalt.|
69494|Barkers Basalt|68344|5|Briefly described|Map legend.|Quaternary|Quaternary||0.26 Ma.||||Olivine basalt.|
69494|Barkers Basalt|68478|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Chudleigh Province.|0.26 Ma||||Olivine basalt.|
69494|Barkers Basalt|68479|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Chudleigh Province.|0.26 Ma||||Olivine basalt.|
69494|Barkers Basalt|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Yates Creek Basalt; the Maer Volcanics; parts of the McBride and Nulla Basalt Groups, and unnamed basalt flows, are all mapped under the symbol, Qbn.||||||
69494|Barkers Basalt|68576|5|Briefly described|Q_11: p20 Fig.17, p29-30|Pleistocene|Pleistocene|Chudleigh Basalt Province, Einasleigh-Mount Surprise area. The Copperfield River cuts a gorge through this unit at Einasleigh. Sourced from Barkers Crater; lava flows c.160km long.|~0.26 Ma (K-Ar).||||A black, highly vesicular flow overlies two other grey, less vesicular flows with prominent cooling columns.|
29309|Barkers Creek Igneous Complex|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
29309|Barkers Creek Igneous Complex|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Divided into Cgox, Ootann Supersuite and Cgok, part Almaden, part Ootann Supersuite.||||||
29309|Barkers Creek Igneous Complex|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 309. I-Type.||||||
29309|Barkers Creek Igneous Complex|23616|5|Briefly described|p99 Appendix 2||Carboniferous|Of Almaden Supersuite.||||||
29309|Barkers Creek Igneous Complex|24485|5|Briefly described|p17 Tb.1, p50 Tb.8|Late Carboniferous|Late Carboniferous|||||||
29309|Barkers Creek Igneous Complex|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
29309|Barkers Creek Igneous Complex|43083|4|Described|p253|||Of Almaden Supersuite.||||||26-AUG-08
29309|Barkers Creek Igneous Complex|43087|2|Defined|p14|Late Carboniferous||||||||
29309|Barkers Creek Igneous Complex|43259|4|Described|Appendix 1,p37.||Carboniferous|||||||
32954|Barkly Group|24303|6|Mentioned|p2|||Invalid name, no longer in use.||||||
32954|Barkly Group|44283|14|Not recorded|p.4|||Ref. to Noakes & Traves, 1947,1954.||||||20-JUL-06
32954|Barkly Group|44285|14|Not recorded|p.4||Cambrian|Ref. to Noakes, 1951, Noakes & Traves, 1954.||||||
32954|Barkly Group|44301|14|Not recorded|p.4||Cambrian|Ref to Noakes 1951, Noakes & Traves 1954.||||||
32954|Barkly Group|44441|14|Not recorded|p.4,9|||Includes rocks now included in Ranken Limestone. Mid.Cam? (E53-16).||||||
32954|Barkly Group|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|||||||
32954|Barkly Group|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|||||||
32954|Barkly Group|64443|1|Redefined|p3, p9-10, p39-40|Middle Cambrian||Originally of Noakes and Traves (1954), including Ogilvie's Georgina Limestone (1931). Note: reinstatement and revised definition of abandoned name. Correlative of Narpa Group in part, lower Goulburn Group, Daly River Group in part, Montejinni Limestone, Hooker Creek Formation, Lothari Hill Sandstone, Point Wakefield beds, Goose Hole Group, Tarrara Formation, Hart Spring Sandstone, Pertaoorrta Group; encompasses all Middle Cambrian sedimentary rocks in the central, western and northern Georgina Basin (except Thorntonia Limestone); previously known as Templeton Series, Georgina Series.|||Includes Top Springs Limestone, Gum Ridge Formation, Anthony Lagoon beds, Wonarah Formation, Ranken Limestone, Camooweal Dolostone.|Unconformably overlies Helen Springs Volcanics or Renner Group or South Nicholson Group; conformably underlies Arrinthrunga Formation.|Limestone, dolostone, siltstone; minor quartz sandstone.|14-MAY-14
32954|Barkly Group|65336|4|Described|Map Legend|Middle Cambrian|Middle Cambrian|Of Georgina Basin. Unconformably overlies Narpa Group; unconformably underlies Brunette Limestone. Includes Camooweal Dolostone, Ranken Limestone, Wonarah Formation.||||||29-SEP-11
32954|Barkly Group|65337|6|Mentioned|p61 Table 6, pp65-68.|Middle Cambrian|Middle Cambrian||||Includes Wonarah Formation, Ranken Limestone and Camooweal Dolostone.|||
32954|Barkly Group|67144|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Top Springs Limestone and Anthony Lagoon Formation.|Unconformably overlies Kiana Group.||13-APR-12
32954|Barkly Group|67148|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge and Wonarah Formations.|||
32954|Barkly Group|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge, Anthony Lagoon and Wonarah Formations.|||
32954|Barkly Group|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge, Anthony Lagoon and Wonarah Formations.|||
32954|Barkly Group|67323|6|Mentioned|GIS attrib tbl, Solid Geology Map.||||||Includes Camooweal Dolomite|||
32954|Barkly Group|67352|4|Described|v, p5, p19, p44 fig 48|Middle Cambrian|Middle Cambrian|Noakes and Traves (1954); Kruse and Radke (2008). Included the Cambrian rocks with rocks in the Hatches Creek tungsten field in this unit.|||Top Springs Limestone, Gum Ridge Formation, Wonarah Formation, Anthony Lagoon Formation|||
32954|Barkly Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
32954|Barkly Group|69443|4|Described|p28:3, 5, 7, 14, 20-25|Middle Cambrian|Middle Cambrian|Noakes and Traves (1954), modified by Kruse and Radke (2008). Barkly and Undilla Sub-basins, Georgina Basin. Includes all Middle Cambrian sedimentary rocks in the central, western and northern Georgina Basin (except Thorntonia Limestone); correlative rocks in the southern and eastern parts of the Basin constitute the Narpa Group. Widely distributed. Correlative of Narpa and Daly River Groups. Is also correlated with the following: lower Goulburn Group (Arafura Basin); Goose Hole Group (Ord Basin); Pertaoorrta Group (Amadeus Basin) in part; Montejinni Limestone, Hooker Creek Formation, Lothari Hill Sandstone and Point Wakefield beds (Wiso Basin); Tarrara Formation, Hart Spring Sandstone, Skewthorpe Formation and Pretlove Sandstone (Bonaparte Basin).|||Gum Ridge, Anthony Lagoon, Wonarah Formations; Top Springs, Ranken Limestones; Camooweal Dolostone.|Unconformably overlies Thorntonia Limestone (Narpa Group) and Helen Springs Volcanics or Renner and South Nicholson Groups. Is overlain conformably by Arrinthrunga Formation.||12-JUL-16
32954|Barkly Group|69591|5|Briefly described|p29, p88|Cambrian|Cambrian|Kruse et al. (2002). Undilla Sub-basin, Georgina Basin.|||Camnooweal Dolostone; Wonarah, Anthony Lagoon, Gum Ridge Formations; Ranken, Top Springs Limestones.|||
32954|Barkly Group|69673|6|Mentioned|p117||||||Includes Gum Ridge Formation, Top Springs Limestone, Anthony Lagoon Formation, Wonarah Formation, Ranken Limestone, Camooweal Dolostone|||
32954|Barkly Group|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Camooweal Dolomite.|||
32954|Barkly Group|72415|4|Described|mapsheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Camooweal Dolomite.|||
32954|Barkly Group|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|||||||
32954|Barkly Group|72919|6|Mentioned|p77|||Georgina Basin. 467 m intersected in drillhole CRDD001.|||Underlain by Helen Springs Volcanics.|||
32954|Barkly Group|72967|6|Mentioned|p5|||Georgina Basin.|||Wonarah Formation, Anthony Lagoon Formation|||
32954|Barkly Group|73083|6|Mentioned|p28||||||Anthony Lagoon Formation|||
36300|Barney Knob Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
36539|Barrabas Granite|23422|5|Briefly described|p176|Devonian|Silurian|Of Barrabas Supersuite.  See also Barrabas Adamellite.||||||
36539|Barrabas Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 197.||||||
34673|Barrabas Supersuite|22847|5|Briefly described|p 13|||||||||
34673|Barrabas Supersuite|23422|4|Described|p176, p214 Table 6.8|||||||||
34673|Barrabas Supersuite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Barrabas supersuite.|||Includes Kedumba and Mount Cuthbert Granodiorites.|||
34673|Barrabas Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
34673|Barrabas Supersuite|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.|||Barrabas Adamellite; Kedumba, Mount Cuthbert Granodiorites.||High-K and high-Rb granitoids.|
34673|Barrabas Supersuite|70740|5|Briefly described|p40|||Granodiorites (Kedumba and Mount Cuthbert) display high K and Rb. |||Includes the Mount Cuthbert Granodiorite and the Kedumba Granodiorite.|||
23363|Barratta Granite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
23363|Barratta Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
23363|Barratta Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 109. Assumed to be I-Type.||||||
23363|Barratta Granite|42245|2|Defined|p41|Permian||||||||
23363|Barratta Granite|43093|6|Mentioned|Table 7|||See also misspelling - Baratta Granite, Appendix 1.||||||
23363|Barratta Granite|43259|4|Described|Appendix 1,p23.|Permian|Carboniferous|||||||
23363|Barratta Granite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
23363|Barratta Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Suite.||||
34681|Barratta Supersuite|22847|5|Briefly described|p 15|||||||||
69313|Barrow Point Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Barrow Point Suite.|||S-type granitoids.|
69314|Barrow Point Suite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains the informally named Barrow Point granite. S-type granites. Detailed lithology presented for the informally named Barrow Point granite.||||||07-FEB-11
69314|Barrow Point Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Barrow Point Granite.||S-type granitoids.|
36181|Bartle Frere Granite|23423|5|Briefly described|p310 Table 7.3||Early Permian|Also see p244. Bartle Frere Supersuite.||||||
36181|Bartle Frere Granite|23497|4|Described|Table 1||Permian|of Bartle Frere Supersuite, Kennedy Province. Previously mapped as part of the Mareeba Granite. I-Type. Age: 264+/-4Ma(Rb/Sr)????. Intrudes Hodgkinson Formation rocks.Unconformably overlain by  basalt corelated with The Fisheries Basalt.||||||
36181|Bartle Frere Granite|23507|5|Briefly described|Map Legend||Early Permian|||||||
36181|Bartle Frere Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 398. I-Type.||||||
36181|Bartle Frere Granite|60425|5|Briefly described|p54 Tb. 4, p83|Permian|Permian|Of the Bartle Frere Supersuite (Bellenden Ker Batholith). I-type biotite granite. Age is probably early Permian? Intruded Hodgkinson Formation.||||||07-FEB-11
36181|Bartle Frere Granite|69079|6|Mentioned|p56|||Mentioned as having some possible relation to quartz float associated with the Kraft Creek gold occurrence.||||||
36181|Bartle Frere Granite|69593|5|Briefly described|p480, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~134 km2 forming Mount Bartle Frere, a granite stock in southern Hodgkinson Province. Sm-Nd isotope data tabulated.|264 +/- 2 Ma.|Bartle Frere Supersuite.|||I-type. (Allanite-) hornblende-biotite and biotite granite and biotite leucogranite.|
36342|Bartle Frere Supersuite|23423|4|Described|p310 Table 7.3||Early Permian|Intrudes Hodgkinson Formation. I-type Granite. Also see p244.||||||
36342|Bartle Frere Supersuite|23497|6|Mentioned|p38|||Sole unit is Bartle Frere Granite. Of Bultitude and Champion (1992).||||||
36342|Bartle Frere Supersuite|60425|3|Fully described|p54 Tb. 4, p85|Permian|Permian|Comprises just Bartle Frere Granite. Age:probably Early Permian? Intruded Hodgkinson Fm. Slightly to moderately porphyritic, hornblende-biotite granite and biotite granite; with minor tourmaline (locally), traces of ilmenite, allanite. I-type.||||||07-FEB-11
36342|Bartle Frere Supersuite|69593|5|Briefly described|p478, p480, p482-483, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~134 km2 forming Mount Bartle Frere, a granite stock in southern Hodgkinson Province.|||Bartle Frere Granite.||I-type. (Allanite-) hornblende-biotite and biotite granite and biotite leucogranite.|
36226|Barwidgi Granite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes Tate Batholith undivided, Gingerella Volcanics. Geological Province: Georgetown Region.||||||24-JUN-15
36226|Barwidgi Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36226|Barwidgi Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 369. I-Type.||||||
36226|Barwidgi Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36226|Barwidgi Granite|23624|5|Briefly described|p18|Permian|Carboniferous|Parent: Ootann Supersuite.||||||08-JUL-15
36226|Barwidgi Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to grey, fine- to medium-grained, moderately porphyritic monzogranite?; locally cut by numerous quartz veins and greisen zones with minor molybdenite and cassiterite?|
36226|Barwidgi Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to grey, fine- to medium-grained, moderately porphyritic monzogranite?; locally cut by numerous quartz veins and greisen zones with minor molybdenite and cassiterite?|
23364|Barwon Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23364|Barwon Granite|22781|4|Described|p32|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
23364|Barwon Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes the Flyspeck Supersuite||||||
23364|Barwon Granite|42610|2|Defined|p8|Early Devonian|Early Devonian|This unit was included in the "Kintore Adamellite" of B135.||||||
23364|Barwon Granite|43738|6|Mentioned|p5|||||||||
23364|Barwon Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
23364|Barwon Granite|71031|6|Mentioned|p26, p33|||||||(Probably) intrudes the Flyspeck Granodiorite.||
23364|Barwon Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Pale grey to cream to brown, fine to medium, muscovite-biotite granite, weakly porphyritic in part.|
35923|Baryulah complex|23359|6|Mentioned|73|||||||||
29200|Batavia Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Transitional deposits between braided fluvial and near shore marine environment.  Of the Gilbert River Formation.||||||
29200|Batavia Member|42061|5|Briefly described|Fig.4 P151|||||||||
29200|Batavia Member|62837|5|Briefly described|Stratigraphic columns|Valanginian|Kimmeridgian|Of the Gilbert River Formation. Age: 140-~133Ma. Geological Province: Northern Cape York.||||||09-NOV-06
77681|Batcha Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Each lithology is separately mapped.||Unit in Ootann Supersuite.|||Pink to white, medium- to fine-grained, moderately porphyritic, leucocratic muscovite-biotite granite, variably altered, locally with K-feldspar phenocrysts to 5 cm; fine-grained monzogranite, extensively weathered, minor muscovite-quartz greisen.|
23365|Bathampton Metamorphics|22543|6|Mentioned|p62|Cambrian|Neoproterozoic|Assigned to Anakie Province||||||22-JUL-15
23365|Bathampton Metamorphics|22557|6|Mentioned|p567,569|||||||||
23365|Bathampton Metamorphics|23078|5|Briefly described|p708|||||||||
23365|Bathampton Metamorphics|23854|5|Briefly described|p857|Neoproterozoic|Neoproterozoic|Of Anakie Metamorphic Group. Geological Province: Anakie Inlier.||||||22-JUL-15
23365|Bathampton Metamorphics|42747|4|Described|p32, Fig.3, Fig.5|||of Anakie Metamorphic Group||||||
23365|Bathampton Metamorphics|43029|6|Mentioned|p12|||||||||
23365|Bathampton Metamorphics|43121|5|Briefly described|p5|||of Anakie Metamorphic Group||||||
23365|Bathampton Metamorphics|43204|5|Briefly described|Map Legend||Neoproterozoic|Neoproterozoic or Early Cambrian. Anakie Inlier||||||23-DEC-11
23365|Bathampton Metamorphics|43213|2|Defined|p8, p10, p20-34, p130-140, p180|||See also p188-190, p202, p204-206, p235, p240, p244. Named after Parish of Bathampton. Outcrops and type area described. Lithofacies described in detail. Geochemistry of mafic rock components detailed. Deformation structures detailed. Altered mafic rocks and ironstone in this unit are associated with the Besshi-type massive sulphide Peak Downs copper deposit, mined between 1863 and 1877; other areas in this unit offer potential for similar mineralisation. Previously mined for lode gold in quartz reefs. Chemical analyses and geophysics detailed.||Basal unit in Anakie Metamorphic Group.|Includes Yan Can Greenstone Member.|Overlain by Theresa Creek Volcanics, Back Creek Group, Blair Athol Coal Measures, Biringam Formation; also Rolfe Creek Schist (structurally). Intruded by Kilmarnock and Mount Newsome Granodiorites.|Lithologically heterogeneous unit; mainly fine-grained mica schist grading into phyllite; white, foliated quartzite is also common; includes laminated greenstones or mafic schist.|
23365|Bathampton Metamorphics|43861|2|Defined|25; Fig1p26; p27-28|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group. Overlies Scurvy Creek Metamorphics, underlies Rolfe Creek Schist.||||||22-JUN-15
23365|Bathampton Metamorphics|66085|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Unit in Anakie Metamorphic Group. White, fine- to coarse-grained, strongly foliated quartzite and fine-grained quartz-mica schist grading to phyllite.||||||
23365|Bathampton Metamorphics|66851|5|Briefly described|p916, 917, 919|||Quartzite units define large-scale F2 folds.|||||Schist, greenstone/serpentinite, quartzite.|18-JAN-17
23365|Bathampton Metamorphics|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.|Includes Yan Can Greenstone Member.|Is conformably overlain by Rolfe Creek Schist.|(Quartz)-mica schist, often grading to phyllite; foliated or laminated greenstone; quartzite.|
23365|Bathampton Metamorphics|68482|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Anakie Province.||Of the Anakie Metamorphic Group.||Conformably overlain by the Rolfe Creek Schist.|Grey, fine to medium-grained mica schist (Rubyvale area), fine-grained quartz-mica schist grading to phyllite (Clermont area) and white, foliated quartzite.|
23365|Bathampton Metamorphics|68731|5|Briefly described|p120, p121, p126, p135, p216|Neoproterozoic|Neoproterozoic|~ 3 km thick. Anakie Province. Withnall et al. (1995).|~ 600-580 Ma, (Fergusson et al. 2001)|Of the Anakie Metamorphic Group.|Includes the Gem Park Granite and the Yan Can Greenstone Member.|Overlain by the Rolfe Creek Schist. Underlain by the Scurvy Creek Meta-arenite. Intruded by the Mount Newsome Granodiorite.|Comprises quartzite, psammite, mica schist, mafic schist, serpentinite, and calc-silicate rocks.|02-JUL-14
23365|Bathampton Metamorphics|68822|6|Mentioned|p320 Fig.3, p323|Cambrian|Cambrian|Charters Towers Province.||||||
23365|Bathampton Metamorphics|68823|5|Briefly described|p404|||Described by Withnall et al. (1995) and Fergusson and Henderson (2013). Mis-spelt as Bathhampton on p404. Deposited pre-Delamerian Orogeny.||Of the Anakie Metamorphic Group.|||Constituents include: pelitic lithofacies; psammitic lithofacies, mainly quartzite; laminated greenstone and calcsilicate rocks interbedded with mica schist; minor serpentine bodies; and massive to foliated metagabbro.|
23365|Bathampton Metamorphics|68900|5|Briefly described|p6, p10|||Drummond Basin.||||Overlain by the Rolfe Creek Schist. Faulted against the Scurvey Creek Meta-arenite.|Fine-grained mica schist grading to phyllite; white, foliated quartzite is also common. Greenstones, metagabbros and mafic schists also occur.|
23365|Bathampton Metamorphics|69541|5|Briefly described|p645 Fig.1(b), p654|Neoproterozoic|Neoproterozoic|||Unit in Anakie Metamorphic Group.|||Heterogeneous unit: mica schist, serpentinite, minor calc-silicate and marble, mafic schist, metagabbro, iron oxide.|
23365|Bathampton Metamorphics|70125|5|Briefly described|p403, p408|||Provenance of 1300-1000 Ma zircons and monazites briefly discussed.|< / = 580 Ma (Fergusson et al., 2001).|Anakie Metamorphic Group.||||
23365|Bathampton Metamorphics|70744|5|Briefly described|p939-941|||Anakie Province. Contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga), likely sourced from the Musgrave Province.|< c.620 Ma.||||Quartzose psammite, pelite, quartzite, amphibolite, mafic schist and serpentinite.|
23365|Bathampton Metamorphics|70749|5|Briefly described|p42-44, p49, p52-53, p55|Cambrian|Neoproterozoic|Anakie Province. Characterised by abundant 1300-900 Ma (late Mesoproterozoic = Grenvillian) aged detrital zircons, and maximum depositional age of ~580 Ma or older. Zircons sourced from Musgrave Province.|~580 Ma (maximum depositional age).|Anakie Metamorphic Group (lower part).||||
23365|Bathampton Metamorphics|70838|6|Mentioned|p276|Ediacaran|Ediacaran|Anakie Inlier.||||||
23365|Bathampton Metamorphics|70856|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|||Anakie Metamorphic Group.|||Grey, fine- to medium-grained mica schist, fine-grained quartz-mica schist grading to phyllite, and white foliated quartzite.|
23365|Bathampton Metamorphics|71966|5|Briefly described|p989-990|Late Neoproterozoic|Late Neoproterozoic|Geological province: Thomson Orogen. Reflects earliest preserved magmatism in the Thomson Orogen.|<580 Ma|Unit of Anakie Metamorphic Group.||Correlable to Mount Arrowsmith Volcanics.|Mafic schists.|
23365|Bathampton Metamorphics|73425|6|Mentioned|p16|Neoproterozoic|Neoproterozoic|Anakie Province, northeast Thomson Orogen.|<620 Ma.|||||
23365|Bathampton Metamorphics|73600|6|Mentioned|p202|||||||||
77211|Bathurst Range Coal Measures|64665|5|Briefly described|p53 Fig.2.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Dalrymple Sandstone. Is overlain by Gilbert River Formation.||
27976|Beapeo Rhyolite|23423|4|Described|p307 Table 7.3||Late Carboniferous|Featherbed Volcanic Group.||||||02-JUN-09
27976|Beapeo Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Featherbed Volcanic Group.||||||
27976|Beapeo Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V118. I-Type.||||||
27976|Beapeo Rhyolite|23616|5|Briefly described|Table 3 p51||Late Carboniferous|Unconformable on Hodgkinson Fm, cut by Worcester Granite and Bulluburrah Granodiorite; probably also predates James Creek Granite. Of Featherbed Volcanic Group. Thickness ~ 300 m.||||||
27976|Beapeo Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Dark grey, welded, crystal-rich to very crystal-rich hornblende-biotite-augite-dacitic ignimbrite; pale to medium grey, welded, lithics-poor to -free, moderately crystal-rich to crystal-rich, hornblende?-biotite rhyolitic ignimbrite.||||||14-DEC-07
27976|Beapeo Rhyolite|43259|4|Described|Appendix 1,p12.||Late Carboniferous|of Featherbed Volcanic Group.||||||
27976|Beapeo Rhyolite|43567|6|Mentioned|Fig.2,p398||Late Carboniferous|||||||
27976|Beapeo Rhyolite|43626|2|Defined|p38||Late Carboniferous|||||||
27976|Beapeo Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27976|Beapeo Rhyolite|60425|4|Described|p48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Gp. Unconformable on Hodgkinson Fm. Cut by Worcester Granite and Bullaburrah Granodiorite. Thickness: ~300m. Pale to dark grey, lithics-poor to -free, moderately crystal-rich to very crystal-rich, dacitic to rhyolitic ignimbrite.||||||07-FEB-11
27976|Beapeo Rhyolite|62523|6|Mentioned|p16 Tb. 1|||On eastern side of Featherbed Cauldron.||||||07-FEB-11
27976|Beapeo Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Three facies are mapped separately, one described as a geophysical variant of the rhyolitic ignimbrite.||Unit in Featherbed Volcanic Group.|||Pale grey, welded rhyolitic ignimbrite with sedimentary rock clasts at base; dark grey, crystal-rich, hornblende-biotite-augite dacitic ignimbrite.|
23371|Beasley Creek Tonalite|22847|3|Fully described|p 52|Early Devonian|Late Silurian|||||||
23371|Beasley Creek Tonalite|23422|6|Mentioned|p210 Table 6.6|||||||||
23371|Beasley Creek Tonalite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23371|Beasley Creek Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 117. I-Type||||||
23371|Beasley Creek Tonalite|42245|2|Defined|p36|Early Devonian|Late Silurian|||||||
23371|Beasley Creek Tonalite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23371|Beasley Creek Tonalite|43259|4|Described|Appendix 1,p23.|Early Devonian|Late Silurian|Late Silurian - Early Devonian?.||||||
23371|Beasley Creek Tonalite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23371|Beasley Creek Tonalite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23371|Beasley Creek Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Beasley Creek ton.||Unit in Millchester Supersuite.||||
75653|Beckford Granodiorite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, medium-grained, moderately porphyritic biotite and hornblende-biotite granodiorite to tonalite; with a weak foliation and traces of allanite.|
36415|Bedarra Granite Complex|23617|4|Described|p21||Carboniferous|Age: 335 Ma (SHRIMP ). Also see p18 Table 2 + Table 3 p52.  In the Kennedy Province.||||||26-AUG-08
36415|Bedarra Granite Complex|23618|5|Briefly described|map legend||Carboniferous|||||||
36415|Bedarra Granite Complex|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit (in part), as well as the Almaden, Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||
36415|Bedarra Granite Complex|69593|5|Briefly described|p491, p495, p512|||Kangaroo Hills and Paluma Subprovinces, Kennedy Igneous Association. Main component of the Bedarra granite belt which forms several islands. Sm-Nd isotope data tabulated.|335 +/- 6 Ma.||||I-type. Dominantly biotite granite; includes hornblende-biotite granite and microgranite; possibly some mafic units.|
36561|Bell Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 229.  I-Type.||||||
24177|Bellenden Ker Granite|12575|6|Mentioned|p784 Table 1.|||Apatite fission track analyses are detailed.|280-228 Ma.|||||
24177|Bellenden Ker Granite|23423|4|Described|p310 Table 7.3||Early Permian|Age: 280 +/- 4 Ma (SHRIMP). S-type Granite. Also see p244. Hodgkinson Province.||||||
24177|Bellenden Ker Granite|23497|5|Briefly described|Table 1||Early Permian|Of Kennedy Province. Intrudes Hodgkinson Formation rocks. Unconformably overlain by The Fisheries Basalt. Age: 280+/-4Ma (SHRIMP)||||||01-JUN-09
24177|Bellenden Ker Granite|23507|5|Briefly described|Map Legend||Early Permian|Age: 280+/-4 Ma SHRIMP.||||||
24177|Bellenden Ker Granite|42625|5|Briefly described|Map legend|Triassic|Late Permian|Reserved.||||||
24177|Bellenden Ker Granite|42810|2|Defined|Table 1 P15|Early Triassic|Late Permian|see also p25.||||||01-JUN-09
24177|Bellenden Ker Granite|43259|6|Mentioned|Appendix 1,p44.||Permian|Part of the Bellenden Ker Batholith.||||||01-JUN-09
24177|Bellenden Ker Granite|60425|4|Described|p10, p56 Tb. 4, p84-85, p274-5 Appdx.1|Early Permian|Early Permian|Of Bellenden Ker Supersuite. Age: 280+/-4ma (SHRIMP).Part intrudes Hodgkinson Fm. Occurs in North Malbon Thompson Range.Coarsely/highly porph.muscovite-biotite granite, extensively sheared (mylonitised), foliated+recrystallised; S-type - more lith.incl.||||||07-FEB-11
24177|Bellenden Ker Granite|69593|5|Briefly described|p480, p482-483|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Main part of the Bellenden Ker Batholith. Forms prominent outcrops between Cairns and Innisfail. U-Pb zircon ages by Bultitude et al. (1997); Garrad and Bultitude (1999); Murgulov (2006).|280.8 +/- 2.1 Ma; 280 +/- 4 Ma; 274.9 +/- 3.3 Ma.||||Porphyritic to even-grained (locally) (tourmaline) muscovite-biotite granite; commonly strongly foliated and partly recrystallised. Reduced I-type.|
69311|Bellenden Ker Suite|60425|5|Briefly described|p274-5 Appdx.1|Early Permian|Early Permian|Of Bellenden Ker Supersuite. Contains Belleneden Ker Granite - S-type, Walshs Pyramid and Mount Peter Granites.||||||05-NOV-20
69312|Bellenden Ker Supersuite|60425|3|Fully described|p56 Tb. 4, p274-5 Appdx.1|Early Permian|Early Permian|Contains Bellenden Ker Suite of granites. Age: 280+/-4ma (SHRIMP). Its granites intruded Hodgkinson Formation. Occurs in northern part of Malbon Thompson Range. Detailed lithology of this porphyritic granite is included. S-type.||||||07-FEB-11
75601|Ben Lomond Granite (QLD)|69594|6|Mentioned|p558|||||||Intrudes Edgecumbe beds.||
35123|Ben Mohr Igneous Complex|23042|4|Described|p45,101,2,3,Fig 2|Early Cretaceous|Late Jurassic|Intrudes the Carmila beds.||||||
35123|Ben Mohr Igneous Complex|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35123|Ben Mohr Igneous Complex|61917|5|Briefly described|Map legend|Cretaceous|Cretaceous|Dark greenish grey, coarse-gr., equigran.biotite-hornblende-pyroxene diorite and gabbro. Pale pink to white, med.to coarse-gr.porphyritic monzogranite grading to pale grey, coarse to v. coarse-gr. porphyritic titanite-biotite-hornblende granodiorite.||||||
35123|Ben Mohr Igneous Complex|65388|2|Defined|p402-405, p136, 143, 364, 365, 410, 420|Early Cretaceous|Early Cretaceous|Intrudes and has strongly hornfelsed Carmila beds. SHRIMP age: 131.8+/-1.6 Ma. Southern Urannah Batholith. Central core consisting dominantly of granitic rocks flanked to the west, north and east by dominantly gabbro and diorite with subordinate granite and granodiorite.||||||
35123|Ben Mohr Igneous Complex|69594|5|Briefly described|p567, p571 Figs.7.46-47|Early Cretaceous|Early Cretaceous|Bowen-Mackay region. Geochemistry plots.|131.8 +/- 1.6 Ma (SHRIMP: Fanning et al. 2009).|||||
35123|Ben Mohr Igneous Complex|71592|5|Briefly described|Appendix A.||||132+/-1.6 Ma (SHRIMP U-Pb zircon).||||Granodiorite.|
82723|Benalla Monzogranite|71628|5|Briefly described|p5: 2; p15: 35, 43, 45-47, 115|Middle Triassic|Early Triassic|Name derived from Benalla homestead. Forms a small (~10 km2) unit ~15 km W of Stanthorpe. Crops out as scattered boulders and pavements. Its ""unique"" geochemistry is described; has similarities with Mount Bullaganang Supersuite granites. Is spatially  associated with (but petrogenetically unrelated to) two Sn deposits.",,||Benalla Suite.||Intrudes Texas beds. Abuts Amiens Leucomonzogranite.|Pale grey to pale pinkish-grey, medium-grained, moderately porphyritic, leucocratic biotite monzogranite; cut by numerous chlorite-rich veinlets and scarce aplite dykes. I-type.|
70403|Benano Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Coarse-grained, highly weathered granite.|
70403|Benano Granite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Coarse-grained syenogranite.|
36493|Bend Pinnacle granodiorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 98.  I-Type.||||||
27075|Bernecker Creek Formation|9541|5|Briefly described|Map legend|Proterozoic|Proterozoic|Weakly metamorphosed calcareous shale, siltstone and sandstone.  Age: Early or Middle Proterozoic.||||||07-JUL-04
27075|Bernecker Creek Formation|22533|6|Mentioned|p55|||In Georgetown Region||||||
27075|Bernecker Creek Formation|22744|5|Briefly described|P7, Table1 P8||Proterozoic|||||||
27075|Bernecker Creek Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates to the Mt Isa Glen Idol Schist and lower sequence of the Willyama Supergroup.||||||07-NOV-08
27075|Bernecker Creek Formation|23032|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27075|Bernecker Creek Formation|23220|5|Briefly described|Fig.2 p9|||of Etheridge Group. Forsayth Subprovince/GI. Overlying unit Daniel Creek Fm (c).||||||
27075|Bernecker Creek Formation|23291|4|Described|p86 Tb.3.6, p22, 23|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Overlying Unit: Daniel Creek Formation. Geological Province: Georgetown Region.||||||18-JUN-15
27075|Bernecker Creek Formation|23425|5|Briefly described|p371|||Etheridge Province.||||||
27075|Bernecker Creek Formation|23430|6|Mentioned|p450|||||||||
27075|Bernecker Creek Formation|23431|5|Briefly described|p530|||Possibly laterally equivalent to Einasleigh Metamorphics.  Of Etheridge Group.||||||
27075|Bernecker Creek Formation|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27075|Bernecker Creek Formation|23494|6|Mentioned|p25 Tb. 1|||On the GILBERTSON Sheet.  See also p24 Tb. 1.||||||
27075|Bernecker Creek Formation|23495|5|Briefly described|map legend||Proterozoic|Age shown as Proterozoic?||||||
27075|Bernecker Creek Formation|24013|5|Briefly described|p19 Tb. 1|Proterozoic|Proterozoic|Calcareous quartz sandstone, calcareous quartz siltstone, impure limestone, calcsilicate hornfels.  Correlated with Lucky Creek Formation.  Max. thickness: 16,000ft.  Overlies and interfingers with Etheridge Fm.  Intruded by Cobbold Dolerite.||||||
27075|Bernecker Creek Formation|30587|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27075|Bernecker Creek Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27075|Bernecker Creek Formation|32528|5|Briefly described|Table 1|||||||||
27075|Bernecker Creek Formation|35811|5|Briefly described|p564|||||||||
27075|Bernecker Creek Formation|35920|6|Mentioned|p26|||||||||
27075|Bernecker Creek Formation|35921|1|Redefined|p31|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
27075|Bernecker Creek Formation|35930|6|Mentioned|Fig.1|||||||||
27075|Bernecker Creek Formation|35948|4|Described|p107|||Deformation and metamorphism P109.||||||
27075|Bernecker Creek Formation|36153|6|Mentioned|Fig.10|||||||||
27075|Bernecker Creek Formation|36780|6|Mentioned|Fig.10|||||||||
27075|Bernecker Creek Formation|37570|4|Described|p115|||See also p109 and p113.||||||03-JUN-15
27075|Bernecker Creek Formation|37571|6|Mentioned|p137|||||||||
27075|Bernecker Creek Formation|37573|6|Mentioned|Fig.12|||||||||
27075|Bernecker Creek Formation|37576|5|Briefly described|p8|||||||||
27075|Bernecker Creek Formation|38714|6|Mentioned|p182|||||||||
27075|Bernecker Creek Formation|39027|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
27075|Bernecker Creek Formation|39445|5|Briefly described|p45|||See also Table 2||||||
27075|Bernecker Creek Formation|39687|6|Mentioned|p1|||||||||
27075|Bernecker Creek Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27075|Bernecker Creek Formation|39924|6|Mentioned|p342|||||||||
27075|Bernecker Creek Formation|41272|5|Briefly described|M 1of1 H06|||||||||
27075|Bernecker Creek Formation|41675|6|Mentioned|p7|||||||||
27075|Bernecker Creek Formation|41680|6|Mentioned|p107|||||||||
27075|Bernecker Creek Formation|41975|3|Fully described|p435|||||||||
27075|Bernecker Creek Formation|42199|5|Briefly described|Table 1 P280|||||||||
27075|Bernecker Creek Formation|43480|6|Mentioned|10-47|||||||||
27075|Bernecker Creek Formation|43664|4|Described|p21-22|||||||||
27075|Bernecker Creek Formation|44043|14|Not recorded|Tb.1,Fig.8,p67|||Conformably overlain by Etheridge Formation.||||||
27075|Bernecker Creek Formation|44045|14|Not recorded|p154|||Unconformably overlain by Gilbert Formation.||||||
27075|Bernecker Creek Formation|44059|14|Not recorded|p444,447||Proterozoic|||||||
27075|Bernecker Creek Formation|45009|14|Not recorded|p29,31-33,62,Tb.2,5||Proterozoic|Metamorphosed unconformably against Einasleigh Metamorphics. Conformably overlain by Etheridge Formation. 10,000'-15,000' thick. Plate 13.||||||
27075|Bernecker Creek Formation|50199|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
27075|Bernecker Creek Formation|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group). Overlain by Daniel Creek Formation. Intruded by Cobbold Metadolerite.||||||07-NOV-08
27075|Bernecker Creek Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||19-AUG-04
27075|Bernecker Creek Formation|61258|5|Briefly described|p386, p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Consists mainly of calcareous and/or dolomitic mudstone, siltstone and fine-grained sandstone. Overlain by Daniel Creek Formation. Geological Province: Georgetown Inlier.||||||07-NOV-08
27075|Bernecker Creek Formation|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
27075|Bernecker Creek Formation|65887|5|Briefly described|p40 Fig.1, p41, p47|Statherian|Paleoproterozoic|Of Etheridge Group.||||||
27075|Bernecker Creek Formation|66800|5|Briefly described|p925, p928, pp932-933.|Proterozoic|Proterozoic|Western subdivision of Etheridge Group. Suggested correlation with Einasleigh Metamorphics.|Probably 1674.9 +/- 3.3 Ma.|Unit in Etheridge Group.||Is overlain by Daniel Creek Formation.|Calcareous and/or dolomitic mudstone, siltstone and fine-grained sandstone; metadolerite and metagabbro sills and small stocks common.|
27075|Bernecker Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Georgetown-Coen-Yambo Inliers.|Protoliths deposited ~1720-1690 Ma.|Lower Etheridge Group.||||
27075|Bernecker Creek Formation|67341|5|Briefly described|vi, p1-4|||Forsayth Subprovince, Etheridge Province. Maximum depositional age.|1844 +/- 11 Ma (SHRIMP U-Pb zircon).|||Is overlain by Daniel Creek Formation.|Includes packages of turbiditic sandstones which have very thick, massive-graded bases, with reworked upper layers.|
27075|Bernecker Creek Formation|67430|6|Mentioned|p25|||||||||
27075|Bernecker Creek Formation|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1670 Ma.|Unit in Etheridge Group.||Is intruded by Cobbold Metadolerite. Is overlain conformably by Daniel Creek Formation (Robertson River Subgroup).|Hornblende and hornblende-diopside gneiss and granofels.|
27075|Bernecker Creek Formation|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1670 Ma.|Unit in Etheridge Group.||Is intruded by Cobbold Metadolerite. Is overlain conformably by Daniel Creek Formation.|Hornblende and hornblende-diopside gneiss and granofels; grades through calcareous mica schist into mudstone, siltstone and fine subfeldspathic sandstone, commonly calcareous and/or dolomitic.|
27075|Bernecker Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.||Interfingers with Einasleigh Metamorphics. Is overlain conformably by Robertson River Subgroup.||
27075|Bernecker Creek Formation|69591|4|Described|p61, p63-64, p67-68, p107|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Crops out in the Gilberton area; at least 2000m thick: base not exposed. In the E it appears to grade, at least in part, into the Einasleigh Metamorphics, parts of which may be stratigraphically lower. Interpreted as turbidites, or wave-dominated shoreline to tidal-flat environments. Contains rare detrital zircons aged ~1695 Ma (Neumann and Kositcin, 2011). Detrital zircon spectra.|~1720-1690 Ma.|Basal Etheridge Group.||Is overlain by Daniel Creek Formation (Robertson River Subgroup).|Predominantly calcareous to dolomitic, fine, subfeldspathic sandstone, siltstone and mudstone; contains a variety of current-related sedimentary structures. Grades E into calcareous mica schist and quartzite, calc-silicate gneiss and granofels.|
27075|Bernecker Creek Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1844+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
27075|Bernecker Creek Formation|71799|5|Briefly described|p150 fig 2, p155 fig 4|Statherian|Statherian|Georgetown area.|ca 1775 Ma|||Overlain by the Daniel Creek Formation.|Sandstone and greywacke.|
27075|Bernecker Creek Formation|72297|6|Mentioned|p728|||Etheridge Province. A minor source of slate; quarries in the Forsayth area.||||||
23380|Berrembea Basalt|24382|5|Briefly described|Map legend|Pleistocene|Pliocene|||||||
23380|Berrembea Basalt|39968|3|Fully described|p85|||||||||
23380|Berrembea Basalt|40542|6|Mentioned|p98|||||||||
23380|Berrembea Basalt|42895|3|Fully described|p80|||Pleistocene age.||||||18-AUG-08
23380|Berrembea Basalt|61155|5|Briefly described|p20|Pleistocene|Pleistocene|Together with Hummock and Barambah Basalts, overlies the Tarraran and Maroondan Melanephelinites. In the Bundaberg-Maryborough region.||||||
23380|Berrembea Basalt|63821|5|Briefly described|p25, p26|Tertiary|Tertiary|Comprises continental olivine basalt and nepheline-bearing olivine basalt.||||||07-FEB-11
23380|Berrembea Basalt|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Barambah and Hummock Basalts, are all mapped under the symbol, Qbs.||||||
23380|Berrembea Basalt|69599|5|Briefly described|p645|Pleistocene|Pleistocene|Gin Gin area. Undated; Pleistocene age is presumed.|||||Small alkaline basalt flows.|
41100|Berri Berri Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41100|Berri Berri Granite|65388|3|Fully described|p244, p236 Fig. 81|Early Permian|Carboniferous|Inferred to intrude the Torsdale Volcanics and to be intruded by the Flat Range Granodiorite. Age tentatively assigned. Could be Late Permian to Early Triassic. Pale grey to very pale pink, medium to fine-grained, uneven-grained to slightly porphyritic (hornblende-) biotite monzogranite. Deeply weathered and partly to extensively decomposed, with sparse relict boulders exposed locally, and deep weathering profiles preserved in places.||||||
41100|Berri Berri Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age range tentative: may be younger.||||Intrudes Torsdale Volcanics. Is intruded by Flat Range Granodiorite.|Medium- to fine-grained to slightly porphyritic (hornblende-)biotite monzogranite.|
38891|Berserker Group|24420|5|Briefly described|p7|Early Permian|Early Permian|||||||
38891|Berserker Group|50207|5|Briefly described|Map Legend|Permian|Early Carboniferous|Includes: Lakes Creek Formation, Chalmers Formation, Ellrott Rhyolite.||||||
38891|Berserker Group|50208|5|Briefly described|Map Legend|Permian|Early Carboniferous|Includes: Chalmers Formation, Ellrott Rhyolite.||||||14-MAY-04
38891|Berserker Group|50209|5|Briefly described|Map Legend|Permian|Permian|Includes: Lakes Creek Formation, Ellrott Rhyolite, Sleipner Member.||||||17-MAY-04
38891|Berserker Group|50212|5|Briefly described|Map Legend|Permian|Permian|Includes Ellrott Rhyolite, Chalmers Formation, Sleipner Member and Lakes Creek Formation.||||||17-MAY-04
38891|Berserker Group|60557|5|Briefly described|p18 Fig. 5a, p25|Early Permian|Early Permian|Overlies the Mount Alma Formation and Rockhampton Group.  See also p19 Fig. 5b.||||||09-JUN-05
38891|Berserker Group|61035|6|Mentioned|p18|Permian|Early Permian|Geological Province: Coastal Block.||||||07-FEB-11
38891|Berserker Group|61778|2|Defined|p233-247, p234 Fig. 1, |Early Permian|Early Permian|Includes; Lakes Creek Formation, Chalmers Formation, Ellrott Rhyolite, Sleipner Member. Overlain by Warminster Formation. Approx thickness: 800m. Geological Province: Berserker Subprovince.||||||07-FEB-11
38891|Berserker Group|63600|5|Briefly described|p919|||Age: 277-268Ma (U-Pb zircon). Located north of Rockhampton.||||||07-FEB-11
38891|Berserker Group|64429|2|Defined|p15-16|Early Permian|Early Permian|Incl:Lakes Creek, Chalmers Fms + Ellrott Rhyolite.Unconform.below Warminster Fm; unconform.on Mount Alma Fm.Mainly marine seds. - siltsts, fine-coarse lithofeldspathic ssts, felsic-intermediate intrusive/extrusive domes, + volc.breccias+ lesser congloms||||||
38891|Berserker Group|68008|3|Fully described|p2, p8, p70, p109, p113, p115, p138-139|Permian|Permian|See also p153, p156-174, p176, p266, p270, p274-275, p307, p426, p480-481, p483-484, p486, p491, p527, p569. Crouch and Parfrey (1998). Originally the Berserker Series of Whitehouse (1930), who regarded them as Devonian, after the Berserker Range. Renamed Berserker beds by Kirkegaard et al. (1970). Part of an extension-related (back-arc) package. Structure and its timing discussed. Hosts Kuroko-style mineralisation at Mount Chalmers. Geochemistry described. Hosts VHMS deposit at Mount Chalmers. Is intruded by Targinie Quartz Monzonite. Is thrust under Princhester Serpentinite.|268.2 +/- 3.9 Ma (U-Pb zircon).||Lakes Creek, Chalmers Formations; Ellrott Rhyolite.|Unconformably overlies Mount Alma Formation and Rockhampton Group. Is overlain by Alton Downs Basalt and Casuarina beds, and unconformably by Warminster Formation. Correlated with Yarrol Formation.|Includes felsic volcanics.|
38891|Berserker Group|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with Double Mountain and Peninsula Range Volcanics, are all mapped under the symbol, Pk.||||||
38891|Berserker Group|68679|4|Described|p312-313, p318, p337-338, p343, p347|Permian|Permian|See also p350, p379, p385, p425, p470. Crouch and Parfrey (1998). Formerly the Berserker beds (Kirkegaard et al., 1970). Crops out as a partly fault-bounded belt ~90km long and up to 15km wide, from Mount Etna S to Mount Larcom. Northern New England Orogen. Previous thickness determination (Kirkegaard et al., 1970) of 3000m is excessive. Previous Devonian age (Whitehouse, 1930) was wrong; the Group contains widespread Permian faunas. Backarc deposits in an extensional regime. May correlate with Wongrabry beds.|||Lakes Creek, Chalmers Formations and Ellrott Rhyolite.|Unconformably overlies Mount Alma Formation and Rockhampton Group. Is overlain unconformably/disconformably by Warminster Formation. (Parts are) intruded by Targinie Quartz Monzonite.|Includes felsic volcanics.|
38891|Berserker Group|69952|6|Mentioned|p75|Permian|Permian|||||||
38891|Berserker Group|73197|5|Briefly described|p474-475, p478, p483|Guadalupian|Cisuralian|New England Orogen, northern. Coeval with Owl Gully Volcanics, Rookwood Volcanics, Double Mountain Volcanics, Peninsula Range Volcanics and Gympie Group. Sediments deposited in a back-arc basin (Crouch, 1999), sequence includes Kuroko-style mineralisation.|277, 276 and 268 Ma U-Pb zircon||||Lavas, pyroclastics and volcanic breccias including abundant silica-rich pyroclastic rocks. Includes sediments and volcaniclastics.|
36548|Berts Dam granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 212.||||||
79719|Betoota beds|70673|5|Briefly described|p10, p27-34||||498 +/- 7 Ma (maximium depositional age).||||Includes red, medium- to coarse-grained lithic sandstone.|
79719|Betoota beds|70749|5|Briefly described|p43-45, p47-51, p55|Cambrian|Cambrian|New, informal name. Undercover Thomson Orogen. Also appears as Betoota Beds in Fig.2 and p51. Fluvial deposits. Lu-Hf and O isotopic results discussed.|498 +/- 7 Ma SHRIMP U/Pb detrital zircon age.||||Steeply dipping (~60-70 degrees) siltstone, lithic sandstone and imbricated polymict conglomerate. Includes red sandstones.|18-JAN-17
79719|Betoota beds|73177|6|Mentioned|p1115 Fig.15, 1116 Tb.2|Ordovician|Cambrian|Thomson Orogen.||||||
28243|Betts Creek beds|23430|5|Briefly described|p519|||||||||
28243|Betts Creek beds|23499|5|Briefly described|map legend|Late Permian|Late Permian|||||||
28243|Betts Creek beds|36472|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
28243|Betts Creek beds|39252|6|Mentioned|p13|||See also P26||||||
28243|Betts Creek beds|39943|6|Mentioned|Table 7A|||||||||
28243|Betts Creek beds|40123|6|Mentioned|p465|||See also Table 2||||||
28243|Betts Creek beds|41116|5|Briefly described|p432|||||||||
28243|Betts Creek beds|41226|6|Mentioned|p22|||||||||
28243|Betts Creek beds|42446|3|Fully described|p9|||||||||
28243|Betts Creek beds|42447|6|Mentioned|Fig.4|||||||||
28243|Betts Creek beds|42474|5|Briefly described|p25|||||||||
28243|Betts Creek beds|43105|5|Briefly described|p13|||||||||
28243|Betts Creek beds|45151|6|Mentioned|p15|||See also P39.||||||
28243|Betts Creek beds|64665|5|Briefly described|pp55-56.|||Galilee Basin. The upper parts of this unit are an extension of the Bandanna Formation, contiguous across the Springsure Shelf. Contains over six billion tonnes of thermal coal, but no commercial exploitation to date (2008). Inertinite (high fusinite) rich. Medium volatile bituminous.||||||
28243|Betts Creek beds|64849|5|Briefly described|Map legend|Permian|Permian|Lithic sandstone, kaolinitic lithic sandstone, micaceous siltstone, conglomerate, mudstone, carbonaceous shale, coal, pebbly mudstone, tuff, breccia.||||||
28243|Betts Creek beds|67323|5|Briefly described|p84, p88-89, p92, p93 Fig.12.3|Permian|Permian|Lovelle Depression, Galilee Basin. Alluvial-coastal plain deposits in a low-accommodation basin setting. Prospective for coal seam gas; also has suitable hydrocarbon reservoir rocks.||||Unconformably overlies Aramac Coal Measures and Boonderoo beds. Is overlain unconformably by Warang Sandstone. Correlated with Bandanna Formation and Colinlea Sandstone.|Includes siltstone and carbonaceous coaly material.|
28243|Betts Creek beds|67402|5|Briefly described|p124 fig GLL1, p125 tbl GLL1|Wuchiapingian|Roadian|Galilee Basin. Sandstones deposited in a braided fluvial environment. See also p127 fig GLL5,p128 fig GLL8, p129 fig GLL9, p132, p134 fig GLL17, p135, p137, p138, p143, p274, p306.||||Unconformably overlies the Aramac Coal Measures. Overlain by the Warang Sandstone.|Fine to coarse-grained, quartzose to sub-labile sandstones interbedded with alluvial and coastal plain coals, siltstones and mudstones.|
28243|Betts Creek beds|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-8, p11, p19|Permian|Permian|Galilee Basin. Appears as Betts Creek Beds on p2, p4, p5 Tb.2, p11, p19. Low energy coal swamps. Galilee Basin stratigraphic cross-sections, and mineralogy tables.|||||Includes tan, silty sandstone consisting of quartz (50%), significant feldspars (24%) and kaolinite (18%).|
28243|Betts Creek beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Galilee Basin.||||||
28243|Betts Creek beds|68679|6|Mentioned|p382|||Galilee Basin. The coal thickens significantly towards the NE margin of the Basin.||||||
28243|Betts Creek beds|68731|5|Briefly described|pp200-203, p223 Fig 3.126|Late Permian|Late Permian|The unconformity between the Betts Creek beds and Warang Sandstone is supported by Palynology. An unconformity surface separates the Betts Creek beds from the Joe Joe Group.||||Unconformably underlain by the Boonderoo beds and the Weston beds. Disconformably overlain by the Warang Sandstone.||
28243|Betts Creek beds|71265|6|Mentioned|p598|||Presented as Betts Creek beds (Group).||||||
28243|Betts Creek beds|71276|3|Fully described|p284-286, p288-294, p297-298|Lopingian|Lopingian|Vine et al. (1964), who thought it was part of the Eromanga Basin; they tentatively expanded its extent to the Muttaburra area. Now designates the whole coal-bearing Lopingian sequence in the northern Galilee Basin; in the south, subdivision is possible. The type section is near the township of Pentland, where the coal seams are restricted to the upper part. Previously the Betts Creek Series of Reid (1916). 46-366m thick. Similar basal conglomerate, sandstone composition, and palynology to Colinlea Sandstone, but separation of > 450km makes correlation questionable. Coal seam correlation. Proposed in this study to upgrade the unit to Betts Creek Group, on the grounds that it can be subdivided using coal-seam correlations.||||Correlative of Bandanna Formation and Colinlea Sandstone.|A lower, conglomeratic part, overlain by Glossopteris-bearing mudstone and kaolinitic and micaceous sandstone, with coal seams.|
28243|Betts Creek beds|71394|5|Briefly described|p1, p8-p16, p21, p24|Late Permian|Lopingian|Galilee Basin. A field transect across this unit is provided and at each stop this unit is described. Plant fossils are identified in this unit. Coal within this unit is very poorly developed.||||Overlain by the Warang Sandstone. Overlies the Boonderoo beds.|Light grey, medium to thick bedded, coarse to very-coarse grained, poorly sorted, pebbly sandstone.|
28243|Betts Creek beds|71701|5|Briefly described|p153, p165|||Elevated in this study to the Betts Creek Group.||||||
28243|Betts Creek beds|71710|4|Described|p367, 370, 376-381, 386|Late Permian|Late Permian|Geological province: Galilee Basin. Base of Betts Creek beds shown gently rolling discontinuity in seismic, suggesting erosion prior to deposition. Onlaps onto basement metamorphic rocks along White Mountains structure. Type location is described. Equivalent units in Galilee Basin recently dated as 254.08+/-0.06 to 252.81+/-0.07 Ma [low uncertainty suggests LA-ICPMS on volcanic units?] Intersected in Towerhill 1, Koburra 1, Thunderbolt 1,Fleetwood 1, Lake Galilee 1 and  Carmichael 1.||With part of Rewan Group, forms sequenece 6, this paper.||Overlain by Rewan Group. Unconformably overlies Aramac Coal Measures, Jochmus Fm. Correlated w Bandanna Fm, Colinlea Sst on palynology; Fair Hill, Burngrove Fms, Black Alley Shale on radiometric age|Basal conglomerate overlain by Glossopteris-bearing mudstone, lithic sandstone and rare tuff interbeds.  Includes thin coal seams.|22-MAY-19
28243|Betts Creek beds|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Galillee Basin.||||||
28243|Betts Creek beds|72088|3|Fully described|p3, p8, p15-p16, p18-p21, p23-p24|Changhsingian|Wuchiapingian|Lovelle Depression, Galilee Basin. Correlated across the basin and into the Denison Trough of the Bowen Basin (Allen and Fielding, 2007a). Extends from outcrop in Porcupine Creek and its type locality in the Pentland area to the southwest along the eastern margin of the Maneroo Platform. The type locality occurs at approximately latitue 20'34'S and 145'15'E at the junction of two branches of Betts Creek. Previously considered correlative to the Colinlea Sandstone and Bandanna Formation. Interpreted to have been deposited on an alluvial plain or in braided channel deposits. See also p30, p38-p40, p42-p44, p72, p91, p94.||||Unconformably overlain by the Warang Sandstone. Unconformably overlies the Jochmus Formation, Aramac Coal Measures and Boonderoo beds.|White to light grey sandstone, siltstone, shale, claystone, coal, carbonaceous shale, conglomerate and minor tuff.|
28243|Betts Creek beds|72297|5|Briefly described|p697, p747, p751|Permian|Permian|Galilee Basin. Contains significant hydrocarbon source rocks. Exploration target for CSG.||||Correlative of Bandanna Formation.|Contains at least two coal seams; sub-bituminous to high-volatile bituminous.|
28243|Betts Creek beds|73472|4|Described|p113-121, p123-124, p126-129...|Olenekian|Wordian|Galilee Basin. A U-Pb LA-ICP-MS zircon age of 251.9 +/- 3 Ma was reported for the Galah Tuff Bed ca 4 m below the top of the unit. A detrital zircon MDA of 267.7 +/- 3.5 Ma is reported for the base of the unit. Maximum thickness of 110 m (GSQ Hughenden 6). Mudstone and coal are more common in the lower portion of the unit. [See article for palynology]. Bracketing zircon ages indicate a depositional interval between ca 267.7 and 251.9 Ma. More locations: p131, App.1, App. 2.|251.9 +/- 3 Ma U-Pb LA-ICP-MS||Galah Tuff Bed|Unconformably underlain by Boonderoo beds and Cape River Metamorphics. Disconformably overlain by Porcupine Gorge Formation. Equivalent to Bandana and Peawaddy fms., Black Alley Sh., and Colinlea Ss.|Pebble to cobble conglomerates, thick white quartzose, cross-bedded sandstones interbedded with siltstones, carbonaceous shales, coal and diamictite.|
36608|Bettsvale granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 402.||||||
23382|Bevandale Granodiorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37.||||||
23382|Bevandale Granodiorite|43029|2|Defined|p19|Late Devonian|Middle Devonian|Rb-Sr dating of 370 Ma. See also Fig.2,p16||||||
23382|Bevandale Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
23382|Bevandale Granodiorite|43213|2|Defined|p96-97, p107-108, p116-121, p175, p177|||See also p208, p211-213, p232, p240, p242. Type locality described. Component of the Retreat Batholith. Rb-Sr biotite-whole rock pair age. Geochemistry, modal analyses and geophysics detailed.|370 +/- 3 Ma (Carr, pers. Comm., 1993).||Intrudes Anakie Metamorphic Group. Is overlain unconformably by Silver Hills Volcanics.||Dominantly grey to light grey, fine- to coarse-grained, subequigranular biotite-hornblende granodiorite.|
23382|Bevandale Granodiorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||370+/-3 Ma Rb-Sr biotite||||Grey, fine to coarse-grained, subequigranular biotite-hornblende granodiorite.|01-SEP-14
24180|Beverly Hills Granite|23430|5|Briefly described|486p|||||||||
24180|Beverly Hills Granite|23619|4|Described|p41 Table 2|||Intrudes Oak River Granodiorite. Also see p7. Copperfield Batholith Province.||||||
24180|Beverly Hills Granite|39981|2|Defined|p104|Devonian|Silurian|Silurian-Devonian. First published as misspelling - Beverley Hills Granite.[CEBMar95]||||||
24180|Beverly Hills Granite|40542|6|Mentioned|p98|||||||||
24180|Beverly Hills Granite|41680|3|Fully described|p124|||||||||
24180|Beverly Hills Granite|43113|4|Described|Table 2,p26.|Early Devonian|Silurian|||||||
24180|Beverly Hills Granite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24180|Beverly Hills Granite|43259|4|Described|Appendix 1,p17.|Early Devonian|Late Silurian|||||||
24180|Beverly Hills Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
36429|Bewilder Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p25. Kennedy Province.||||||
26390|Biarraville Formation|23799|3|Fully described|p32, p14 Tb. 1|Permian|Permian|Of Cressbrook Creek Group.  Overlain by Box Gully Formation; underlain by Hampton Road Rhyolite. Geological Province: Cressbrook Creek Province.  Max. thickness: 50m (45m in type section).  Intruded by "Champion Hills Diorite".||||||09-APR-08
26390|Biarraville Formation|23800|5|Briefly described|Map legend|Permian|Permian|Of the Cressbrook Creek Group.||||||
26390|Biarraville Formation|24560|5|Briefly described|Map legend|Permian|Permian|Of Cressbrook Creek Group.||||||
26390|Biarraville Formation|32945|6|Mentioned|p90|||Permian||||||
26390|Biarraville Formation|33381|4|Described|p108|||See also p111. of the Cressbrook Creek Group.||||||09-APR-08
26390|Biarraville Formation|33711|6|Mentioned|Table 3|||||||||
26390|Biarraville Formation|39252|6|Mentioned|Fig.13|||||||||
26390|Biarraville Formation|39445|6|Mentioned|Chart 6,2|||||||||
26390|Biarraville Formation|42525|5|Briefly described|Map legend|Early Permian?|Early Permian?|Of the Creesbrook Creek Group.||||||15-JUL-04
26390|Biarraville Formation|43475|14|Not recorded|p553||Permian|||||||
26390|Biarraville Formation|44555|2|Defined|p224||Permian|See also Lexicon. Conformably overlies Hampton Road Rhyolites.||||||
26390|Biarraville Formation|61782|5|Briefly described|p278|||Of Cressbrook Creek Group. Limestones and has fossiliferous horizon. Formation is evidence of mass flow and perhaps a slope environment.||||||
26390|Biarraville Formation|68679|5|Briefly described|p385-386|Guadalupian|Guadalupian|Cranfield et al. (2001). Cressbrook Basin. Marine, shallow-water deposits. <50m thick. Richly fossiliferous (species listed).||Cressbrook Creek Group.||Unconformably overlies Hampton Road Rhyolite. Is overlain unconformably by Box Gully Formation. May correlate with South Curra Limestone.|Chert, sandstone, siltstone, mudstone, sedimentary breccia, rhyolite, crinoidal limestone, coarse-grained andesitic conglomerate;  richly fossiliferous horizons.|
36217|Big Bend Formation|23422|5|Briefly described|p180|Middle Devonian|Middle Devonian|Of Fanning River Group. Also referred to as Big Bend Arkose on p206 Table 6.3.||||||
36217|Big Bend Formation|23430|5|Briefly described|p505|||Of Fanning River Group.||||||
36217|Big Bend Formation|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|of Fanning River Group.||||||
36217|Big Bend Formation|23893|5|Briefly described|p16|Middle Devonian|Middle Devonian|Of Fanning River Group.  Geological Province: Burdekin Basin.||||||
36217|Big Bend Formation|24613|5|Briefly described|p9 Fig. 4|Eifelian|Eifelian|Probably misspelt - see Big Bend Arkose.||||||07-FEB-11
36217|Big Bend Formation|67402|4|Described|p239, p246, p247, p248|Eifelian|Eifelian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a marine (inner shelf) environment. ||Fanning River Group||Overlain  by the Burdekin Formation.|Predominantly feldspathic (arkosic) calcareous sandstone with interbedded siltstone, sandy limestone and rubbly calcirudite; lesser intercalated conglomerate, sandstone and siltstone also occurs.|
36217|Big Bend Formation|68731|5|Briefly described|p177 Fig 3.91, p183, p185 Tb 3.4|Middle Devonian|Middle Devonian|Burdekin Basin. < 90 m thick. Near-shore transgressive fluvial to shoreface facies with siliciclastic components derived from erosion of the underlying basement. Large gastropods are characteristic but a diverse fauna is represented by bioclasts.||Of the Fanning River Group.|||Comprises boulder to cobble conglomerate, coarse to very coarse arkosic sandstone, locally pebbly or with pebble lags, siltstone. Bioclasts occur in some intervals.|
36217|Big Bend Formation|69030|5|Briefly described|p6|Devonian|Devonian|Camel Creek Subprovince (Broken River Province).||Fanning River Group.||||
36217|Big Bend Formation|71031|5|Briefly described|p56|Middle Devonian|Middle Devonian|Burdekin Basin. ||Fanning River Group||Overlies the Mount Success Rhyolite.|Fine- to medium-grained arkose sandstone.|
31108|Big Bore Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31108|Big Bore Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
31108|Big Bore Granodiorite|43480|2|Defined|11-15|Devonian|Silurian|||||||
31108|Big Bore Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
76111|Big Supersequence|62535|5|Briefly described|p672-673|Statherian|Statherian|Calvert Superbasin.|c.1730? Ma.|||Is overlain unconformably by Prize Supersequence. Correlated with lower Willyama Supergroup.||
76111|Big Supersequence|63112|6|Mentioned|p1191 Fig.2|||Calvert Superbasin.||||||
76111|Big Supersequence|63114|5|Briefly described|p1253 Fig.2.|||Calvert Superbasin.|||Includes Fiery Creek Volcanics and Bigie Formation.|Is overlain by Prize supersequence.||
76111|Big Supersequence|63866|6|Mentioned|p53|||Calvert Superbasin.||||||
76111|Big Supersequence|65228|5|Briefly described|p21, p25, Figs.10, 12-14.|||Calvert Superbasin. Gamma ray log, lithology and facies detailed.||||||
76111|Big Supersequence|65337|6|Mentioned|p32.|||Southgate et al (2000) and Page et al (2000) includes an older (c.1700 Ma) component of Surprise Creek Formation in this Supersequence.||||||
76111|Big Supersequence|67323|5|Briefly described|p11, p24, p39|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Calvert Superbasin. Mount Oxide Domain, Mount Isa Inlier. Fluvial to shallow marine deposits.|~1730-1705 Ma.||Comprising Bigie Formation, Fiery Creek Volcanics.|Overlies Quilalar Supersequence. Is overlain by Prize Supersequence.||
76111|Big Supersequence|68021|5|Briefly described|p135 Fig 4|Statherian|Statherian|Calvert Superbasin. Equivalent to Surprise Creek Formation. Environment changing from near-shore to deltaic or shallow marine. |~1710 - ~1705 Ma||Includes Fiery Creek Volcanics, Bigie Formation.|||
76111|Big Supersequence|68146|6|Mentioned|p203|||Lawn Hill Platform, Murphy Inlier and Southern McArthur Basin regions, Calvert Superbasin. Experienced volcanism and plutonism at c.1740-1730 Ma.||||||
76111|Big Supersequence|68732|5|Briefly described|p159, p161, p166, p171|||Includes Fiery Creek Volcanics, Bigie Formation, Weberra Granite, Deighton Quartzite (unit 1), Mitakoodi Quartzite, Stavely Formation and Doherty Formation.||||||
76111|Big Supersequence|69591|6|Mentioned|p27, p37-38, p106|||Mount Isa Province. Includes Bigie Formation and Fiery Creek Volcanics.||||||
76111|Big Supersequence|72912|6|Mentioned|p13.|Paleoproterozic|Paleoproterozic|Of Calvert Superbasin. Comprising a complex of northeast trending half grabens (Derrick 1982; O'Dea et al., 1997;  Betts et al., 2006; Gibson et al., 2008; Gibson et a., 2017).|||Fiery Creek Volcanics, Peters Creek Volcanics and Bigie Formation ?||Includes volcanics.|
76111|Big Supersequence|73144|4|Described|p9-10, p39, p42-43|Statherian|Statherian|Sequence Stratigraphy. Calvert Superbasin. High lateral variability. Divided into a basal conglomerate and an overlying sandstone; the contact between which is gradational and interbedded. Counted as basement in the thermal history model reported herein.|1705-1730 Ma|||Includes Bigie Formation and Fiery Creek Volcanics.|Volcanics, conglomerates and siliciclastics.|
27037|Big Surprise Tuff|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Agate Creek Volcanic Group. Geological Province: Georgetown Region.||||||25-MAY-15
27037|Big Surprise Tuff|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V29. I-Type.||||||
27037|Big Surprise Tuff|39917|6|Mentioned|Map legend|Permian|Permian|||||||
27037|Big Surprise Tuff|40542|6|Mentioned|p97|||||||||
27037|Big Surprise Tuff|40860|6|Mentioned|Table 2|||||||||
27037|Big Surprise Tuff|43259|4|Described|Appendix 1,p3.||Permian|of Agate Creek Volcanic Group.||||||
27037|Big Surprise Tuff|43740|4|Described|p30, 77||Carboniferous|Includes info on contacts, thickness||||||01-SEP-04
27037|Big Surprise Tuff|50199|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Agate Creek Volcanic Group.||||||
27037|Big Surprise Tuff|50210|5|Briefly described|Map Legend|Permian|Permian|Of the Agate Creek Volcanic Group.||||||
27037|Big Surprise Tuff|50211|4|Described|Map Legend|Early Permian|Early Permian|Of Agate Creek Volcanic Group. Overlain by Talaveras Rhyolite.||||||17-MAY-04
27037|Big Surprise Tuff|68353|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Is overlain conformably by Talaveras Rhyolite.|Grey, green or brown crystal and lithic-rich rhyolitic volcanic arenite to very coarse polymictic volcanic rudite with basement lithic clasts.|
27037|Big Surprise Tuff|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Is overlain conformably by Talaveras Rhyolite.|Grey, green or brown crystal and lithic-rich rhyolitic volcanic arenite to very coarse polymictic volcanic rudite with basement lithic clasts.|
27037|Big Surprise Tuff|68415|5|Briefly described|Map Legend|Permian|Permian|Early Permian age. Of the Kennedy Province.||Unit in Agate Creek Volcanic Group.|||Grey, green, or brown basement-derived and locally volcanic lithic arenite to rudite; maar or diatreme fill.|
80892|Big Tableland Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Big Tableland Suite.|||S-type granitoids.|
36725|Big Tableland Suite|23423|5|Briefly described|Table 7.1 p240|||Of Collingwood Group.||||||
36725|Big Tableland Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains the informally named Big Tableland granite. S-type. Detailed lithology included.||||||07-FEB-11
36725|Big Tableland Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Big Tableland Granite||S-type granitoids.|
25784|Big Toby Granite|22795|5|Briefly described|p69|||||||||
25784|Big Toby Granite|23545|5|Briefly described|Fig 1 p604|||||||||
25784|Big Toby Granite|31342|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
25784|Big Toby Granite|32660|5|Briefly described|Table 5|||||||||
25784|Big Toby Granite|32959|6|Mentioned|Fig.21|||||||||
25784|Big Toby Granite|33900|5|Briefly described|p21|||Mention P7||||||
25784|Big Toby Granite|35074|6|Mentioned|Fig.2|||||||||
25784|Big Toby Granite|35167|2|Defined|p151|Middle Precambrian|Middle Precambrian|||||||
25784|Big Toby Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
25784|Big Toby Granite|38232|6|Mentioned|p83|||||||||
25784|Big Toby Granite|38900|6|Mentioned|p62|||||||||
25784|Big Toby Granite|39445|5|Briefly described|Table 2|||Age 1800 Ma. See also P40||||||
25784|Big Toby Granite|39934|6|Mentioned|Fig.3|||||||||
25784|Big Toby Granite|40840|6|Mentioned|Map legend|||||||||
25784|Big Toby Granite|41298|6|Mentioned|Map legend|Proterozoic||||||||
25784|Big Toby Granite|41465|6|Mentioned|p8|||||||||
25784|Big Toby Granite|41466|6|Mentioned|p23|||||||||
25784|Big Toby Granite|41978|6|Mentioned|p501|||||||||
25784|Big Toby Granite|42367|5|Briefly described|p17|||Age U-Pb zircon 1800 Ma||||||
25784|Big Toby Granite|42565|5|Briefly described|Table 2 P7|||||||||
25784|Big Toby Granite|42706|5|Briefly described|map legend|Paleoproterozoic|Palaeoproterozoic|Age: ~1800Ma. Biotite granite.||||||09-FEB-09
25784|Big Toby Granite|43608|6|Mentioned|Fig.11,p11|||||||||
25784|Big Toby Granite|45166|5|Briefly described|p33|||||||||
25784|Big Toby Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25784|Big Toby Granite|48997|6|Mentioned|Fig.3|||||||||
25784|Big Toby Granite|49041|5|Briefly described|Table 1|||||||||
25784|Big Toby Granite|61922|6|Mentioned|p21 Fig. 13|||||||||
25784|Big Toby Granite|61929|5|Briefly described|p128 Fig. 2|||||||||
25784|Big Toby Granite|61933|5|Briefly described|p169 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1800 Ma. Intrudes the Yaringa Metamorphics.||||||07-NOV-08
25784|Big Toby Granite|61936|6|Mentioned|p193|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
25784|Big Toby Granite|63866|6|Mentioned|p58|||According to the author this is also known as the Monoghans Granite.||||||
25784|Big Toby Granite|64249|5|Briefly described|p82 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1800Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
25784|Big Toby Granite|64250|5|Briefly described|p9 fig 1, p11 fig 3, p19, p21|||Western Fold Belt, Mount Isa Inlier. Preceded the accumulation of the Leichhardt Superbasin (c.1800-1750 Ma).|~1800 Ma|||||
25784|Big Toby Granite|65396|6|Mentioned|p11,p82,p103,p172,p175,p187,p192,p241|Orosirian|Orosirian|Its emplacement preceded the accumulation of the Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform.|c.1800 Ma|||||
25784|Big Toby Granite|66824|6|Mentioned|p137|||Problems with previous age determinations discussed.||||||
25784|Big Toby Granite|67323|4|Described| p6,10, p23; GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Ardmore-May Downs Domain, Mount Isa Inlier. Post-Barramundi Orogeny; Big Toby Igneous Event (intraplate magmatism). Intrusion 1820-1800 Ma.|~1810 - 1795 Ma|Big Toby Suite||Intrudes Yaringa Metamorphics. Age correlation with Monaghans and Yeldham Granites|Adamellite, medium biotite granite, minor foliated coarse granite and syenite|
25784|Big Toby Granite|68146|4|Described|p1, p6, p63-68, p194, p211|||Mount Isa Region. Poorly exposed series of angular bouldery outcrops. Occurs W of the May Downs Fault. The unusual texture may result from brittle tectonic activity, followed by silicification and recrystallisation. Previous age determination given. Coeval with Paper Tank Microgranite and Bottletree Formation volcanics. Whole-rock Sm-Nd isotopic data tabulated.|1795 +/- 5 Ma magmatic/emplacement age.|||Adjacent to Sybella Granite.|Massive to weakly gneissic, orange to brick red silicified microgranite; characteristic rounded to subangular "eyes" of quartz; thin, discontinuous veins of milky quartz.|
25784|Big Toby Granite|68575|5|Briefly described|p53|||Yaringa Creek, W margin of the Sybella Batholith. Originally mapped as Sybella Granite.|1795 +/- 5 Ma (Carson et al., 2011).|||Is overlain by Torpedo Creek Quartzite.|Pink microgranite.|
25784|Big Toby Granite|69222|5|Briefly described|p222 Fig.2, p224 Fig.3, p225 Tb.2, p226|||Kalkadoon-Leichhardt Fold Belt. At least 5km thick (based on seismic data). Heat flow values given.|1804 +/- 15 Ma|||Intrudes Leichhardt Volcanics||09-FEB-18
25784|Big Toby Granite|69591|5|Briefly described|p30, p32|||Ardmore-May Downs Domain, Mount Isa Province.|1795 +/- 5 Ma (Carson et al., 2011).|Big Toby Suite.||Intrudes Yaringa Metamorphics.|Medium biotite granite, minor foliated coarse granite and syenite.|
25784|Big Toby Granite|71606|6|Mentioned|p137|Statherian|Statherian| Leichardt River Fault Trough, Mount Isa Inlier.||||||
25784|Big Toby Granite|71960|5|Briefly described|p77|Paleoproterozoic|Paleoproterozoic|Basement to Mount Isa Group.|1804 Ma U-Pb zircon.|||||
25784|Big Toby Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
25784|Big Toby Granite|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1795+/-5 Ma crystallisation age||||Felsic intrusion.|
25784|Big Toby Granite|73529|6|Mentioned|p15 Fig.11||||1800 Ma|||||
25784|Big Toby Granite|73553|6|Mentioned|p259|Statherian|Statherian|Western Fold Belt.|1795+/-5 Ma (Carson et al., 2011)|||||
31421|Big Toby Suite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
31421|Big Toby Suite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince  (Mount Isa Orogen).||||||07-NOV-08
31421|Big Toby Suite|67323|5|Briefly described|p11, p107; GIS attrib tbl|||See also, Solid Geology Map. |||Big Toby Granite, Monaghans Granite|||
31421|Big Toby Suite|69591|6|Mentioned|p60||||||Big Toby, Little Toby, Monaghans Granites.|||
29325|Bilch Creek Granodiorite|23423|6|Mentioned|p239|||||||||
29325|Bilch Creek Granodiorite|23713|5|Briefly described|p73 Appendix 2|||Intrudes Nightflower Dacite, Hodgkinson Formation.||||||
29325|Bilch Creek Granodiorite|43087|2|Defined|p88|Late Carboniferous||||||||
29325|Bilch Creek Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).||||||15-JUN-06
29325|Bilch Creek Granodiorite|43254|5|Briefly described|map legend||Late Carboniferous|of Almaden Supersuite.||||||
29325|Bilch Creek Granodiorite|43259|4|Described|Appendix 1,p37.||Late Carboniferous|||||||
29325|Bilch Creek Granodiorite|43625|6|Mentioned|p49|||||||||
29325|Bilch Creek Granodiorite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite. Geological Province: Kennedy Province. Pale to medium-grey, fine to medium-grained, highly porphyritic biotite-hornblende granodiorite to monzogranite; commonly altered.||||||31-MAY-04
29325|Bilch Creek Granodiorite|60425|4|Described|p49 Tb.3, p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Intruded Nightflower Dacite (Featherbed Volcanic Group). I-type. Pale to medium grey, fine- to medium grained, highly porphyritic augite-biotite-hornblende granodiorite to granite; commonly altered.||||||07-FEB-11
23386|Billings Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|O'Briens Creek Supersuite.||||||
23386|Billings Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite. Age: ~314Ma Rb-Sr.||||||01-JUN-09
23386|Billings Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 268. I-Type.||||||
23386|Billings Granite|23616|5|Briefly described|p75|||Of O'Briens Creek Supersuite. Tate Batholith.||||||
23386|Billings Granite|41235|6|Mentioned|p42|||See also Fig. 2a.||||||14-NOV-14
23386|Billings Granite|41740|6|Mentioned|p222|||||||||
23386|Billings Granite|43060|5|Briefly described|p101|||Of O'Briens Creek Supersuite.||||||29-APR-09
23386|Billings Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Pale grey to pink, fine to coarse, even-grained to variably porphyritic biotite granite to microgranite. Age: 314Ma.||||||29-APR-09
23386|Billings Granite|43259|4|Described|Appendix 1,p35.||Carboniferous|||||||
23386|Billings Granite|60425|4|Described|p284-5 Appdx.|||Of Nettle Suite (O'Briens Creek Supersuite). Fine- coarse-gr., even-gr.to variably porphyritic, biotite granite-microgranite + sheet-like distribution; with associated Sn mineralisation. Age probably Late Carboniferous as for most  Nettle Suite granites||||||07-FEB-11
23386|Billings Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pale grey to pink, fine- to coarse-grained, even-grained to variably porphyritic, biotite syenogranite; with sheet-like form.|
80919|Billy Hill Granite|69592|5|Briefly described|p283|||Copperfield Batholith. Unassigned.|||||Muscovite-biotite leucogranite to leucogranodiorite; biotite leucogranite. Probably I-type (no analytical data).|
36629|Billy-Can Creek Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 485.  I-Type.||||||
36629|Billy-Can Creek Granite|60659|5|Briefly described|p18|||Pink porphyritic microgranite to very fine-grained granite.  Intrudes the Locharwood Rhyolite.||||||07-FEB-11
36629|Billy-Can Creek Granite|70740|5|Briefly described|p84, p85, p105, p120-p122|||Distribution is briefly discussed on p122. ||||Intrudes the Hidden Valley Rhyolite.|Pink, slightly porphyritic, fine-grained monzogranite that is leucocratic and miarolitic and relatively homogenous.|
27038|Bimba Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27038|Bimba Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 801. S-Type.||||||
27038|Bimba Granite|24197|5|Briefly described|p77, p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralada Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
27038|Bimba Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27038|Bimba Granite|40659|6|Mentioned|p250|||||||||
27038|Bimba Granite|40954|6|Mentioned|p132|||||||||
27038|Bimba Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
27038|Bimba Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
27038|Bimba Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Medium- to fine-grained garnet-biotite granite; porphyritic.||||||13-OCT-08
27038|Bimba Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium- to fine-grained garnet-biotite granite; porphyritic, commonly with ophitic, needle or plate-like biotite phenocrysts; some graphite pellets.|
27038|Bimba Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium- to fine-grained garnet-biotite granite; porphyritic, commonly with ophitic, needle or plate-like biotite phenocrysts; some graphite pellets.|
27038|Bimba Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Coarse biotite granite with trace secondary muscovite; contains garnet.|
23388|Bimurra Volcanics|22675|4|Described|p16|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
23388|Bimurra Volcanics|22800|5|Briefly described|Fig.2 p581, p591|Late Devonian|Late Devonian|||||||
23388|Bimurra Volcanics|23052|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
23388|Bimurra Volcanics|23161|4|Described|p10,11 table2a|Early Carboniferous|Late Devonian|Age: 356+/-5Ma.||||||
23388|Bimurra Volcanics|23430|6|Mentioned|p510|||Drummond Basin Province||||||
23388|Bimurra Volcanics|23513|5|Briefly described|Map legend|Carboniferous|Devonian|Palaeozoic Volcanic No. V78.||||||18-JUL-13
23388|Bimurra Volcanics|41825|6|Mentioned|p205|||||||||
23388|Bimurra Volcanics|42054|6|Mentioned|p272|||||||||
23388|Bimurra Volcanics|42474|6|Mentioned|p29|||Mount Coolon 1:250 000 sheet.||||||
23388|Bimurra Volcanics|42701|3|Fully described|p21|Late Devonian||||||||
23388|Bimurra Volcanics|43259|4|Described|Appendix 1,p8.||Late Carboniferous|U-Pb zircon age is 297+/-2 Ma.||||||
23388|Bimurra Volcanics|43391|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Geological Province: Drummond Basin. Late Devonian and/or Early Carboniferous.  Dacitic ignimbrite.||||||23-JUN-04
23388|Bimurra Volcanics|43727|5|Briefly described|p1|||||||||
23388|Bimurra Volcanics|43734|6|Mentioned|p6|||'superseded'||||||
23388|Bimurra Volcanics|44245|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
23388|Bimurra Volcanics|60659|4|Described|p10, p58|Fammenian|Fammenian|Basal andesitic volcanics overlain by trachyandesitic to trachytic lava and tuff. Underlie Mount Wyatt Formation; unconformably overlain by Bobby Dazzler Rhyolite also. Age: 356+/-2.9Ma. Geological Province: Drummond Basin.||||||07-FEB-11
23388|Bimurra Volcanics|65668|5|Briefly described|p1, p2 Tb.1, p8-10|Early Carboniferous|Late Devonian|Drummond Basin. Age 360.2 +/- 2.5 Ma (SHRIMP U-Pb zircon). Thick sequence of lava and tuff: basal andesitic volcanics, overlain by trachyandesite to trachyte lava and tuff that grades upwards into rhyolitic volcanics and interbedded sediments.||||||
23388|Bimurra Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Foyle, Silver Hills and Stones Creek Volcanics, and the Mount Wyatt and Saint Anns Formations, are all mapped under the symbol, DCD1.||||||
23388|Bimurra Volcanics|68679|5|Briefly described|p363-364|Mississippian|Late Devonian|Drummond Basin.|360.2 +/- 2.5 Ma (SHRIMP: Cross et al., 2009)||||Rhyolite lava.|
23388|Bimurra Volcanics|68705|6|Mentioned|p41|Tournaisian|Famennian|Includes a rhyolite lava (now dated) that may host mineralisation.|360.2 +/- 2.5 Ma U/Pb SHRIMP|||||
23388|Bimurra Volcanics|68731|5|Briefly described|p128, p191 Fig 3.102, p192, p193|Mississippian|Late Devonian|Hutton et al. (1991). Up to 4 km thick. Locally extensive siliceous sinter deposits are developed within this succession, reflecting activity of hydrothermal springs during deposition. Geochronology by Perkins, Walshe and Morrison (1995).|356.2 +/- 2.9 Ma, U-Pb|||Conformably overlies the Mount Wyatt Formation (in the far north) but underlies it in southwest BOWEN area. Unconformably underlain by the Les Jumelles beds.|Comprises andesitic volcanics at the base overlain by trachyandesite to trachytic lava and volcaniclastics that grade upwards into rhyolitic to dacitic volcanics with minor sedimentary interbeds including volcanilithic conglomerate.|11-MAY-16
23388|Bimurra Volcanics|68900|5|Briefly described|p4, p18|Late Devonian|Late Devonian|Drummond Basin.||||Unconformably overlies the Les Jumelles beds.||
23388|Bimurra Volcanics|68901|6|Mentioned|p3|Early Carboniferous|Late Devonian|||||||
23388|Bimurra Volcanics|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|||||||
23388|Bimurra Volcanics|70740|3|Fully described|i, ii, iii, p7, p8, p20, p24, p29-p32|Early Carboniferous|Late Devonian|First defined by Hutton et al, 1991, replacing parts of the Mount Rankin beds and Bulgonunna Volcanics or the Mount Wyatt Formation. SHRIMP age is derived from Cross et al, 2009. Additional SHRIMP ages from Ivey (1999) and Perkins et al (1995) are given on p8. These ages are corroborated by lycopsids fossil assemblage. Mistakenly referred to as the Bimurra Volcanics Formation on p31 and as the Mount Bimurra Volcanics on p29. Distribution, outcrop characteristics, structure, geochemistry and type area/type section are discussed. Lithology and petrography at several locations are described in detail. Estimated thickness ranging from 3500m to 4000m with a preserved thickness of 400-500m in the type area. Fig 27 (p53) provides a geological map of the proposed type area. Often difficult to distinguish from the Mount Wyatt Formation. Unconformably overlain by the Bulgonunna Volcanic Group and Suttor Formation. Overlain by the Pyramid Rhyolite. Equivalent to the Saint Anns Formation, Silver Hills Volcanics and Stones Creek Volcanics. Partially equivalent to the Mount Wyatt Formation. Intruded by the Bluestone Creek Granodiorite, Roscow Granite and the Percy Douglas Tonalite. See also p34, p41-p44, p46-p60, p62-p76, p83, p86-p89, p92, p94 fig 55, p116-p118, p124, p128, p129.|360.2 +/- 2.5 Ma (SHRIMP U-PB)|||Conformably overlies the Mount Wyatt Formation. Unconformably overlies the Les Jumelles beds. Overlies the Ukalunda Formation.|Rhyolitic lava, quartz-feldspar porphyry and rhyolitic ignimbrite. Volcaniclastic sediments including mudstone, fine-grained sandstone, siltstone and thick-bedded, poorly sorted cobble conglomerate.|
23388|Bimurra Volcanics|71592|5|Briefly described|Appendix A.|||Drummond Basin.|360+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
23388|Bimurra Volcanics|73035|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Two informal subunits recognised. Some polygons of this unit are uncertainly identifed.|||||Coherent and autoclastic rhyolite, locally strongly flow banded; comprises numerous lava flows with significant textural variation on 10's of metres scale; minor intercalated volcaniclastic sediments. Coherent + autoclastic dacitic to andesitic lavas|
23388|Bimurra Volcanics|73197|6|Mentioned|p465 Fig.4|Carboniferous|Carboniferous|Drummond Basin.|||||Volcanics.|
80765|Binbee Quartz Monzodiorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, medium-grained, uneven-grained biotite-hornblende quartz monzodiorite to quartz diorite?; with minor clinopyroxene, traces of titanite; extensively deformed and partly recrystallised with a well-developed foliation in most places.|
36223|Bird Spring Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36223|Bird Spring Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 366. I-Type.||||||
36223|Bird Spring Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36223|Bird Spring Granite|23624|4|Described|p14|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||08-JUL-15
36223|Bird Spring Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pale pink to white, medium to coarse-grained, even-grained biotite granite.||||||07-FEB-11
36223|Bird Spring Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to white, medium- to coarse-grained, even-grained biotite granite.|
36223|Bird Spring Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to white, medium- to coarse-grained, even-grained biotite granite.|
32075|Birdbush Basalt Flow|23509|5|Briefly described|Map Legend||Quaternary|Informal name.||||||
32075|Birdbush Basalt Flow|43933|5|Briefly described|Map Legend||Quaternary|||||||
32075|Birdbush Basalt Flow|73115|6|Mentioned|p: 76, 90, 94, 99, 105, 110, 115, 120|||See also Birdbush Basalt p75, 77||||||
75646|Birds Nest Granodiorite|68679|5|Briefly described|p362|Mississippian|Mississippian|Northern Connnors Subprovince. Well-developed foliation.|327.9 +/- 2.4 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75646|Birds Nest Granodiorite|68901|5|Briefly described|p4, p54-56, p145|Carboniferous|Carboniferous|Northern New England Orogen, Bowen Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|327.9 +/- 2.4 Ma (SHRIMP U-Pb)||||Pale grey, medium to fine-grained, slightly porphyritic hornblende-biotite granodiorite.|15-NOV-18
75646|Birds Nest Granodiorite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Pale grey, fine to medium-grained, uneven-grained to slightly porphyritic hornblende-biotite granodiorite; foliated and partly recrystallised; with minor titanite; mafic inclusions up to c. 10 cm across are common.|
24183|Birds Well Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24183|Birds Well Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24183|Birds Well Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24183|Birds Well Granite|37862|4|Described|p585|||||||||
24183|Birds Well Granite|38310|6|Mentioned|p237|||||||||
24183|Birds Well Granite|38350|4|Described|p17|||||||||
24183|Birds Well Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24183|Birds Well Granite|39445|5|Briefly described|Table 2|||||||||
24183|Birds Well Granite|40840|6|Mentioned|Map legend|||||||||
24183|Birds Well Granite|45161|5|Briefly described|p31|||||||||
24183|Birds Well Granite|45166|5|Briefly described|p34|||||||||
24183|Birds Well Granite|49009|2|Defined|p4|Proterozoic|Proterozoic|Previously mapped as Kalkadoon Granite (Carter & Opik,1963).||||||11-OCT-22
24183|Birds Well Granite|49041|5|Briefly described|Table 2|||||||||
24183|Birds Well Granite|50100|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Wonga Suite. Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||
24183|Birds Well Granite|50536|5|Briefly described|p1.4, 5.2 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.||||||07-NOV-08
24183|Birds Well Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite granite; minor gneiss, augen gneiss.||||||
24183|Birds Well Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Medium to coarse biotite granite, strongly foliated to massive.|
24183|Birds Well Granite|69591|5|Briefly described|p60|||Wonga Batholith.|||||Medium to coarse biotite granite; strongly foliated to massive.|
24183|Birds Well Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent  equivalent age to other Wonga Suite units and Burstall Suite units.|Medium to coarse biotite granite, strongly foliated to massive with deeply weathered bedrock, in some areas.|
24183|Birds Well Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Medium to coarse biotite granite, strongly foliated to massive with deeply weathered bedrock, in some areas.|
24183|Birds Well Granite|73137|4|Described|p1, p5, p88-94|||[Previously known exposures of the unit are written as Birds Well Granite or Birds Well Granite proper]. A sample from further south than other known exposures was examined herein [written as Birds Well Granite? to denote uncertain assignment]. This sample produced a magmatic crystallisation age of 1863 +/- 6 Ma (similar to units from the Kalkadoon-Leichhardt Domain). The sampled unit intrudes the Plum Mountain Gneiss of similar age, which suggests the Birds Well Granite? is part of the basement assemblage; however, previously known exposures [Birds Well Granite proper] have cross-cutting relationships that implying an age younger than 1775-1780 Ma, which suggests similarities with the younger Mary Kathleen Domain. [Although Birds Well Granite proper and Birds Well Granite? appear to have conflicting cross-cutting relationships, the authors report that the available data suggest the two units could be correlatives]. [See article for Birds Well Granite? field description, petrographic description and detailed geochronology].|<~1775-1780 Ma OR 1863 +/- 6 Ma|Wonga Suite||Intrudes Magna Lynn Metabasalt and Argylla Formation.|Includes biotite granite.|
24183|Birds Well Granite|73413|6|Mentioned|p5|||[Also written as Birdwell granite].||||||
24183|Birds Well Granite|73553|4|Described|p1, p6, p8, p14, p18, p36, p43-45|Orosirian|Orosirian|Included in Kalkadoon-Leichhardt Igneous Province based on imprecise U-Pb zircon (LA-ICP-MS) date, and a SHRIMP zircon date of 1863+/-6 Ma tentatively assigned to the unit. Mapped as part of Kalkadoon Granite by Carter et al., (1961), subsequently delineated as a discrete, younger unit. Formerly assigned to the Wonga Suite by Budd et al., (2001), more recent geochronology implies the unit is older than the Wonga-Burstall Igneous Province. Comprises an elongate NW to northerly aligned pluton ~33 km long and ~3.5 km wide. Mottled pink to red tones on radiometric images. Low responses on aeromagnetic images. Fault bounded to the west. Reported to intrude Leichhardt Volcanics and Kalkadoon Granite, tentatively correlated with Bowlers Hole Granite (Blake et al., 1981a, b; Bultitude et al., 1982a). Cut by numerous non-foliated to foliated metadolerite dykes. A-type. See also  p47, p49-50, p59, p63-54, p80-81, p157-158, p243-250, p253, p257.|1863+/-6 Ma U-Pb zircon SHRIMP|Wonga Suite||Intrudes Magna Lynn Metasbasalt, Argylla Formation, possibly Saint Mungo Granite|Pale grey-pale pink, fine- to medium-grained, slightly-moderately porphyritic biotite granite containing scattered phenocrysts of white to pale pink feldspar|03-FEB-23
24184|Birimgan Formation|41737|2|Defined|p358|Middle Permian||||||||
24184|Birimgan Formation|42054|6|Mentioned|p272|||||||||
24184|Birimgan Formation|43204|5|Briefly described|Map Legend|Late Permian|Late Permian|Moorlands Basin||||||21-DEC-11
24184|Birimgan Formation|43213|5|Briefly described|p34, p154, p157-158|Permian|Permian|Sorby and Scott (1988). Moorland Basin. A coal resource of 28 Mt was inferred but has limited economic importance due to low rank and high sulphur content.||||Overlies Bathampton Metamorphics. Correlated with Ingelara Formation and Catherine Sandstone.|Mostly fine- to medium-grained sandstone, dominantly quartzose, with common cross-bedding and ripple marks; with interbeds of mudstone, siltstone and coal.|
24184|Birimgan Formation|43861|5|Briefly described|25,28||Permian|||||||
24184|Birimgan Formation|68412|5|Briefly described|Map legend|Permian|Permian||||||Sandstone, shale, mudstone, quartz-pebble to polymictic conglomerate and coal.|
36317|Bismark Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36317|Bismark Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pink to pale grey, fine- to medium-grained, slightly porphyritic (hornblende?-)biotite monzogranite.|25-MAR-15
33437|Bjelke Petersen beds|23799|3|Fully described|p24, p15 Tb. 1|||Originally "Wondai Series" (Reid, 1925).  Parts included in the superseding "Wondai Metamorphics" of Derrington (1954).  Age: 314-311Ma (Namurian-Westphalian).  Geol. Prov: Yarraman Subprovince.||||||19-OCT-12
33437|Bjelke Petersen beds|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
33437|Bjelke Petersen beds|60371|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince. Mudstone, shale and silicified siltstone.||||||
33437|Bjelke Petersen beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Yarraman Subprovince. This unit, as well as Maronghi Creek beds, Fifer Creek, Sugarloaf and Mountefontein Metamorphics, and unnamed sedimentary units, are all mapped under the symbol, DCym.||||||
24726|Black Alley Shale|13516|5|Briefly described|p145 fig 3, p146 fig 4, p147 fig 5|Late Permian|Late Permian|From Denison Trough, Roma Shelf, Taroom Shelf, Comet Ridge of Bowen Basin, also Galilee Basin. Age APP5005 -APP5006 and includes the P3c acritarch horizon.||||||
24726|Black Alley Shale|22601|2|Defined|401, 414, 415|Permian|Permian|Geol province Bowen Basin. Underlying unit Peawaddy Formation||||||
24726|Black Alley Shale|22872|5|Briefly described|p535, Fig.1 p536|Early Triassic|Late Permian|||||||
24726|Black Alley Shale|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
24726|Black Alley Shale|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
24726|Black Alley Shale|22978|6|Mentioned|p148 Fig.1|||||||||
24726|Black Alley Shale|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
24726|Black Alley Shale|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
24726|Black Alley Shale|23444|5|Briefly described|p190|||||||||
24726|Black Alley Shale|24069|5|Briefly described|p284|Permian|Permian|Geological Province: Surat Basin.||||||
24726|Black Alley Shale|24071|5|Briefly described|p317 Table 1|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
24726|Black Alley Shale|24077|5|Briefly described|p410 Tb. 2|Late Permian|Late Permian|Of the Blenheim Subgroup.  Includes the Winathoola Coal Member.  Max. thickness: 190m.  Geological Province: Bowen Basin.  See also p411 Tb. 3.||||||
24726|Black Alley Shale|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: >251Ma.  Geological Province: Bowen Basin.||||||
24726|Black Alley Shale|24160|6|Mentioned|p18|||At Mantuan Downs, SW of Springsure; hosts bentonite deposits.||||||
24726|Black Alley Shale|29391|6|Mentioned|Table 3|||See P18 & also Table 4 on P19||||||
24726|Black Alley Shale|29393|6|Mentioned|Table 2|||Permian.||||||
24726|Black Alley Shale|29409|6|Mentioned|Table 1|||Equated with lower part of Burngrove Fm.||||||
24726|Black Alley Shale|29410|5|Briefly described|p273|||Also correlation diagram on P275.||||||
24726|Black Alley Shale|29411|5|Briefly described|p201|||||||||
24726|Black Alley Shale|29721|6|Mentioned|p65|||||||||
24726|Black Alley Shale|30141|6|Mentioned|p135|||||||||
24726|Black Alley Shale|30448|6|Mentioned|p100|||||||||
24726|Black Alley Shale|30450|6|Mentioned|Table 1|||Permian||||||
24726|Black Alley Shale|30508|6|Mentioned|p91|||Palynology||||||
24726|Black Alley Shale|30546|6|Mentioned|p107|||Upper Permian age. Correlation||||||
24726|Black Alley Shale|30691|4|Described|p14|||See also p21,Table 3,6. Upper Permian age.||||||06-SEP-18
24726|Black Alley Shale|30826|6|Mentioned|p634|||||||||
24726|Black Alley Shale|30854|6|Mentioned|p8|||||||||
24726|Black Alley Shale|30915|6|Mentioned|Table|||Shown on Table for Stratigraphic drilling||||||
24726|Black Alley Shale|30916|6|Mentioned|p98|||||||||
24726|Black Alley Shale|31120|4|Described|p153|||||||||
24726|Black Alley Shale|31122|6|Mentioned|p352|||||||||
24726|Black Alley Shale|31260|6|Mentioned|p16|||Facies analysis||||||
24726|Black Alley Shale|31303|5|Briefly described|p292|||See also Table 1||||||
24726|Black Alley Shale|31305|4|Described|p570|||Mention Table 1||||||
24726|Black Alley Shale|31369|6|Mentioned|p3|||||||||
24726|Black Alley Shale|31531|5|Briefly described|p11|||U.Permian. See also Table 1||||||
24726|Black Alley Shale|32139|6|Mentioned|p583|||||||||
24726|Black Alley Shale|32493|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
24726|Black Alley Shale|32577|6|Mentioned|p23|||U.Perm. See also P24||||||
24726|Black Alley Shale|32578|4|Described|p352|||||||||
24726|Black Alley Shale|32689|6|Mentioned|Fig.2|||Refers Power (1967)||||||
24726|Black Alley Shale|32840|6|Mentioned|Fig.1,30|||Stratigraphy & biostratigraphy.||||||
24726|Black Alley Shale|33059|4|Described|Table 1|||U.Perm.||||||
24726|Black Alley Shale|33078|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24726|Black Alley Shale|33079|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24726|Black Alley Shale|33086|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24726|Black Alley Shale|33366|6|Mentioned|Fig.3|||Perm.||||||
24726|Black Alley Shale|33368|6|Mentioned|p12|||Well log.||||||
24726|Black Alley Shale|33369|6|Mentioned|p214|||Strat. succession at Jericho 1.||||||
24726|Black Alley Shale|33530|5|Briefly described|Table 1|||||||||
24726|Black Alley Shale|33639|6|Mentioned|Fig.1|||||||||
24726|Black Alley Shale|33640|5|Briefly described|Table 4|||||||||
24726|Black Alley Shale|33646|6|Mentioned|p10|||Correlation. Palynological stage.||||||
24726|Black Alley Shale|33648|6|Mentioned|p17|||Palynological divisions.||||||
24726|Black Alley Shale|33675|4|Described|p412|||Lithology.||||||
24726|Black Alley Shale|34132|6|Mentioned|p2|||Upper Permian||||||
24726|Black Alley Shale|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
24726|Black Alley Shale|34174|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
24726|Black Alley Shale|34408|6|Mentioned|p185|||On Table||||||
24726|Black Alley Shale|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
24726|Black Alley Shale|35016|6|Mentioned|p41|||||||||
24726|Black Alley Shale|35079|6|Mentioned|Fig.3|||||||||
24726|Black Alley Shale|35138|6|Mentioned|p16|||||||||
24726|Black Alley Shale|35148|4|Described|p414|||See also Table 1.||||||
24726|Black Alley Shale|35150|6|Mentioned|p422|||||||||
24726|Black Alley Shale|35266|6|Mentioned|p202|||||||||
24726|Black Alley Shale|35433|6|Mentioned|p27|||||||||
24726|Black Alley Shale|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
24726|Black Alley Shale|35467|6|Mentioned|p178|||||||||
24726|Black Alley Shale|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
24726|Black Alley Shale|35845|6|Mentioned|Fig.25|||||||||
24726|Black Alley Shale|35873|6|Mentioned|Fig.25|||||||||
24726|Black Alley Shale|35901|6|Mentioned|p2|||||||||
24726|Black Alley Shale|36103|4|Described|Table 1|||||||||
24726|Black Alley Shale|36104|6|Mentioned|p122|||||||||
24726|Black Alley Shale|36233|5|Briefly described|p157|||See also Table 1.||||||
24726|Black Alley Shale|36241|4|Described|p125|||||||||
24726|Black Alley Shale|36243|6|Mentioned|Table 3A|||||||||
24726|Black Alley Shale|36739|6|Mentioned|p10|||||||||
24726|Black Alley Shale|36921|6|Mentioned|p175|||||||||
24726|Black Alley Shale|37070|6|Mentioned|p69|||||||||
24726|Black Alley Shale|37072|6|Mentioned|p90|||||||||
24726|Black Alley Shale|37450|6|Mentioned|p374|||||||||
24726|Black Alley Shale|37610|6|Mentioned|Fig.3|||||||||
24726|Black Alley Shale|37705|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|37724|6|Mentioned|Table 1|||||||||
24726|Black Alley Shale|37726|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|37749|6|Mentioned|p186|||||||||
24726|Black Alley Shale|37858|6|Mentioned|p85|||||||||
24726|Black Alley Shale|38092|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|38312|4|Described|p462|||||||||
24726|Black Alley Shale|38603|6|Mentioned|p81|||||||||
24726|Black Alley Shale|38955|4|Described|p315|||||||||
24726|Black Alley Shale|39212|4|Described|p34|||Excursion site described. See also p11 & p35||||||06-SEP-22
24726|Black Alley Shale|39219|6|Mentioned|p46|||Microflora||||||
24726|Black Alley Shale|39252|6|Mentioned|Fig.13|||||||||
24726|Black Alley Shale|39261|6|Mentioned|Fig.6|||||||||
24726|Black Alley Shale|39263|6|Mentioned|Fig.1|||||||||
24726|Black Alley Shale|39264|6|Mentioned|Fig. 4|||||||||
24726|Black Alley Shale|39267|6|Mentioned|p240|||||||||
24726|Black Alley Shale|39268|6|Mentioned|p269|||||||||
24726|Black Alley Shale|39272|5|Briefly described|p295|||Correlation||||||
24726|Black Alley Shale|39273|6|Mentioned|Fig. 2|||||||||
24726|Black Alley Shale|39275|6|Mentioned|p332|||||||||
24726|Black Alley Shale|39412|6|Mentioned|p1|||||||||
24726|Black Alley Shale|39423|6|Mentioned|Fig.1|||||||||
24726|Black Alley Shale|39445|5|Briefly described|Table 8|||See also P101||||||
24726|Black Alley Shale|39494|6|Mentioned|Fig.5|||||||||
24726|Black Alley Shale|39611|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|39666|6|Mentioned|p115|||||||||
24726|Black Alley Shale|39777|6|Mentioned|p153|||||||||
24726|Black Alley Shale|39815|6|Mentioned|Fig.10|||||||||
24726|Black Alley Shale|39943|6|Mentioned|Table 5A|||||||||
24726|Black Alley Shale|40030|6|Mentioned|Fig.5|||||||||
24726|Black Alley Shale|40093|6|Mentioned|p40|||||||||
24726|Black Alley Shale|40123|6|Mentioned|Table 2|||||||||
24726|Black Alley Shale|40249|6|Mentioned|p41|||||||||
24726|Black Alley Shale|40250|6|Mentioned|Table 6|||||||||
24726|Black Alley Shale|40256|6|Mentioned|p306|||||||||
24726|Black Alley Shale|40321|6|Mentioned|p19|||||||||
24726|Black Alley Shale|40539|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|40544|6|Mentioned|Fig.6|||||||||
24726|Black Alley Shale|40675|6|Mentioned|Table 7A|||||||||
24726|Black Alley Shale|40687|6|Mentioned|Table 3|||||||||
24726|Black Alley Shale|41173|6|Mentioned|p91|||||||||
24726|Black Alley Shale|41246|6|Mentioned|Map legend|Permian||||||||
24726|Black Alley Shale|41247|6|Mentioned|Fig.7|||||||||
24726|Black Alley Shale|41330|6|Mentioned|Table 1|||||||||
24726|Black Alley Shale|41475|6|Mentioned|Fig.1|||||||||
24726|Black Alley Shale|41605|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|41725|6|Mentioned|Fig.2|||||||||
24726|Black Alley Shale|41809|6|Mentioned|p63|||||||||
24726|Black Alley Shale|42067|4|Described|Appendix 2|||See also Fig.2 p309||||||06-SEP-22
24726|Black Alley Shale|42091|6|Mentioned|p284|||||||||
24726|Black Alley Shale|42249|6|Mentioned|p23|||||||||
24726|Black Alley Shale|42250|6|Mentioned|Fig.4 P31|||||||||
24726|Black Alley Shale|42251|6|Mentioned|Fig.2 P38|||||||||
24726|Black Alley Shale|42253|5|Briefly described|Fig.2 P217|||||||||
24726|Black Alley Shale|42254|6|Mentioned|p221|||||||||
24726|Black Alley Shale|42309|6|Mentioned|p303|||||||||
24726|Black Alley Shale|42437|6|Mentioned|Fig.3 P822|||||||||
24726|Black Alley Shale|42578|5|Briefly described|Table 1 P124-125|||||||||
24726|Black Alley Shale|42611|6|Mentioned|p11|||||||||
24726|Black Alley Shale|42641|5|Briefly described|p109|||||||||
24726|Black Alley Shale|42662|6|Mentioned|p84 Fig.4|||||||||
24726|Black Alley Shale|42856|5|Briefly described|Fig.2 P632|||||||||
24726|Black Alley Shale|42865|5|Briefly described|p18|||||||||
24726|Black Alley Shale|42911|5|Briefly described|p10|||||||||
24726|Black Alley Shale|43000|5|Briefly described|p113|||see also Fig.5,p112||||||
24726|Black Alley Shale|43017|5|Briefly described|Fig.3,p375|||||||||
24726|Black Alley Shale|43050|5|Briefly described|Fig.1,p5|||||||||
24726|Black Alley Shale|43105|6|Mentioned|p13|||||||||
24726|Black Alley Shale|43185|5|Briefly described|6,10||Late Permian|||||||
24726|Black Alley Shale|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
24726|Black Alley Shale|43812|6|Mentioned|Fig.3,p145|||||||||
24726|Black Alley Shale|43982|14|Not recorded|Map Legend|||||||||
24726|Black Alley Shale|43990|14|Not recorded|Map Legend|||Part of Blenheim Sub-Group.||||||
24726|Black Alley Shale|43994|14|Not recorded|Map Legend|||||||||
24726|Black Alley Shale|44022|14|Not recorded|Map Legend||Late Permian|||||||
24726|Black Alley Shale|44023|4|Described|Tb.2,p7||Late Permian|||||||
24726|Black Alley Shale|44172|2|Defined|p1339,143,1327-8,||Kazanian|p1330,1334,Tb.1. Denison Trough||||||
24726|Black Alley Shale|44173|14|Not recorded|p110 (Fig.1)||Late Permian|||||||
24726|Black Alley Shale|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
24726|Black Alley Shale|44421|14|Not recorded|p10|||||||||
24726|Black Alley Shale|44424|14|Not recorded|p293-301|||Part of Blenheim Subgroup; apparently equivalent to Macmillan Member.||||||
24726|Black Alley Shale|44787|14|Not recorded|p124|||||||||
24726|Black Alley Shale|44824|14|Not recorded|unknown (p347-350)|||||||||
24726|Black Alley Shale|45031|14|Not recorded|p9||Permian|||||||
24726|Black Alley Shale|45071|3|Fully described|p55|||See also Table 10||||||
24726|Black Alley Shale|45095|6|Mentioned|p9|||See also Table 2. Refers Mollan et al. (1969)||||||
24726|Black Alley Shale|45110|4|Described|Table 16|||See also Table 13.||||||
24726|Black Alley Shale|46849|6|Mentioned|p192|||||||||
24726|Black Alley Shale|46989|5|Briefly described|Table 1|||||||||
24726|Black Alley Shale|48898|6|Mentioned|Fig.27|||U.Permian. Blenheim Subgroup||||||
24726|Black Alley Shale|48900|2|Defined|p39|Late Permian|Late Permian|||||||
24726|Black Alley Shale|48919|5|Briefly described|p18|||U.Permian||||||
24726|Black Alley Shale|48920|3|Fully described|p28|||Upper Permian age||||||
24726|Black Alley Shale|48995|6|Mentioned|Fig.3|||||||||
24726|Black Alley Shale|49644|5|Briefly described|Table|||||||||
24726|Black Alley Shale|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
24726|Black Alley Shale|60286|4|Described|p275 Fig.2|Late Permian|Late Permian|Overlies Peawaddy Formation. Overlain by Bandanna Formation. Deposited in a restricted basin. Geological Province: Bowen Basin.||||||
24726|Black Alley Shale|60330|5|Briefly described|p261 Fig.2|Tatarian|Tatarian|||||||
24726|Black Alley Shale|61612|6|Mentioned|p272, p277, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
24726|Black Alley Shale|62357|5|Briefly described|p524 Fig. 7|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
24726|Black Alley Shale|62921|6|Mentioned|p878 Fig.2|Wuchiapingian|Wuchiapingian|shown as in SE Galilee Basin and Bowen Basin.||Unit in Blackwater Group.||||24-AUG-15
24726|Black Alley Shale|63713|5|Briefly described|p1507-1508, p1523, p1525-1526, p1533|Wuchiapingian|Capitanian|See also p1528-1531. Bowen Basin and eastern margin, Galilee Basin. A maximum-flooding event. Graphic log. Well-log correlation.|||Includes Winnathoola Coal Member.|Overlies Peawaddy and Tinowon Formations. Is overlain by Bandana Formation.||
24726|Black Alley Shale|63832|6|Mentioned|p131 fig 2|Lopingian|Guadalupian|Of Galilee Basin.||||||
24726|Black Alley Shale|63978|5|Briefly described|p7|Early Triassic|Late Permian|Ages: 250.1+/-2.8Ma and 250.1+/-2.2Ma (Roberts et al 1996, 1997). Geological province: Bowen Basin.||||||07-FEB-11
24726|Black Alley Shale|64288|5|Briefly described|p532 Fig.1 |Wuchiapingian|Campanian|||||Overlies Peawaddy Formation. Is overlain by Bandanna Formation.||
24726|Black Alley Shale|64631|5|Briefly described|p44 Fig.2, p48 Fig.4.|Wuchiapingian|Capitanian|Galilee and Bowen Basins. Biostratigraphic age control for base and top.||||Overlies Peawaddy Formation. Is overlain by Bandanna Formation.||
24726|Black Alley Shale|64856|4|Described|p42, p65-68, p64 Fig.13|Late Permian|Late Permian|Mollan et al. (1969); previously the lower part of the Bandanna Formation of Hill (1957). Bowen Basin. Conformably overlies Mantuan Productus bed, the Tinowon Formation in the Taroom Trough and Roma Shelf and Peawaddy Formation in Denison Trough. Overlain by Bandanna Formation. Correlated with Burunga and Wiseman Fms. Contains the Winnathoola Coal Member. Shale, siltstone, tuff, coal; minor sandstone. Age from palynoflora (unit APP5).Up to 358m thick.| | ||||28-NOV-17
24726|Black Alley Shale|64857|5|Briefly described|p121-124, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Overlies Peawaddy Formation.||||||
24726|Black Alley Shale|64858|5|Briefly described|p182, p181 Tb.1, p180 Fig.2, p186 Fig.10|Late Permian|Late Permian|Bowen Basin. Includes Winnathoola Coal Member.||||||30-NOV-09
24726|Black Alley Shale|64859|6|Mentioned|p196, 225|Permian|Permian|Oil and gas source rocks.||||||
24726|Black Alley Shale|65112|5|Briefly described|p315, fig 4 p314|Late Permian|Late Permian|Part of Supersequence F. In West of Bowen-Gunnedah-Sydney Basin system in the Denison Trough. 4 Ma sequence up to 500 m thick in east. This unit is called the Burunga Formation in East (Taroom Trough).||||Underlies Bandanna Formation; overlies Peawaddy Formation.||22-MAR-12
24726|Black Alley Shale|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian|Denison Trough. Overlies Peawaddy Formation underlies Bandanna Formation.||||||24-AUG-15
24726|Black Alley Shale|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
24726|Black Alley Shale|65115|5|Briefly described|p418-419, Fig 2 p403|Permian|Permian|Dark marine shelf muds. Minimal fauna/flora. Underlies the Bandanna Formation in the Denison Trough, Bowen Basin. Part of Supersequence F.||||||
24726|Black Alley Shale|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Bandanna Formation, overlies the Peawaddy Formation, Denison Trough, Bowen Basin.||||||06-MAR-12
24726|Black Alley Shale|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Bandanna Formation, overlies the Peawaddy Formation in the Denison Trough, Bowen Basin.||||||
24726|Black Alley Shale|66188|6|Mentioned|431|||Transgressive||||||
24726|Black Alley Shale|66615|6|Mentioned|p2 Fig.1, p3-5, p7 Fig.4, p8 Fig.5|||Denison and Southern Taroom Trough, Bowen Basin.||||||
24726|Black Alley Shale|67402|4|Described|p18 fig WSD2, p21|Wuchiapingian|Capitanian|Bowen Basin. Deposited in a restricted marine to lacustrine environment. Proven gas seal and potential hydrocarbon seal. Poor potential to be a Carbon Dioxide seal as it is generally <800m deep. Generally less than 50m thick. See also p23 fig CTM3, p45, p48, p52, p53, p56, p64, p65, p66 fig BWW4, p68, p69, p72, p73, p124 fig GLL1, p125, p132, p134 fig GLL17, p136, p141, p300. ||||Overlain by the Bandanna Formation. Overlies the Tinowon, Peawaddy and Muggleton Formations.|Shale, siltstone, tuff and coal.|
24726|Black Alley Shale|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Bandana Formation. Equivalent to Winnathoola, Fort Copper or Gyranda Coal Measures.||
24726|Black Alley Shale|68279|5|Briefly described|p2, p4, p5 Tb.2, p7, p9-10, p16 Tb.4|Lopingian|Lopingian|See also p17-19. Springsure Shelf, S Galilee Basin and Denison Trough, Bowen Basin. Deposited under brackish-marine conditions in a basin with limited direct access to the sea. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Overlies Peawaddy Formation.|A succession of black mudstones with white tuff beds.|
24726|Black Alley Shale|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||Of the Back Creek Group.||Unconformably overlain by the Blackwater Group. Conformably underlain by the Peawaddy Formation.|Mudstone, siltstone, tuff and sandstone.|
24726|Black Alley Shale|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||Of the Back Creek Group.||Overlain by the Blackwater Group. Conformably underlain by the Peawaddy Formation.|Mudstone, siltstone, tuff and sandstone.|
24726|Black Alley Shale|68576|5|Briefly described|Q_4: p3, p10-11, p20, p24|Lopingian|Lopingian|Bowen Basin. Brackish-marine conditions, with deposition ending in a restricted freshwater lake.||||Conformably overlies Peawaddy Formation. Is overlain by Bandanna Formation or Rewan Group.|Grey to black, silty, tuffaceous, carbonaceous shale, generally micaceous with minor pyrite, coal, siltstone and minor sandstone, with thin white to cream tuffaceous beds. Bioturbation common.|
24726|Black Alley Shale|68679|5|Briefly described|p377, p381-383|Permian|Permian|Mollan et al. (1969). Denison Trough, Bowen Basin. 358m thick. Lacustrine, pro-delta deposits.||||Overlies Peawaddy and Tinowon Formations. Passes laterally into the Burngrove Formation. Is overlain by Bandanna Formation.|Mudstone, siltstone, numerous tuff beds; coal present on the Roma Shelf.|
24726|Black Alley Shale|68731|6|Mentioned|p201 Fig 3.110|Early Triassic|Early Triassic||||||Comprises dark grey to black shale and siltstone with interbedded light green-grey tuff and fine to very fine, labile sandstone.|
24726|Black Alley Shale|70857|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group||Overlies Peawaddy Formation|Mudstone, siltstone, tuff and sandstone.|
24726|Black Alley Shale|70861|4|Described|p36-41,45|Late Permian|Late Permian|Of Bowen Basin. Also called Black Alley Shale Formation on p41. Deposited in a marine, transgressive setting.||Unit of Fort Cooper Coal Measures.||Overlain by, and interfingers with Middle Main Seams and Burngrove Formation. Underlain by Fair Hill Formation.|Multiple fining and coarsening upward siltstone and mudstone, overlain by medium sorted and clean coarsening upward sandstone.|19-AUG-19
24726|Black Alley Shale|70878|4|Described|p705, p717, p720 Fig.15, p725|Permian|Permian|Bowen Basin. A SHRIMP age determination of 250.1 +/- 2.8 Ma by Roberts et al. (1996), allowing this unit a late Permian or Early Triassic age, is discussed with reference to a more recent CA-IDTIMS age of 252.2 +/- 0.4 Ma for the overlying Rewan Group (Mundil et al., 2006)[now Rewan Formation]. Immediately overlying tuff, at the base of the Kaloola Member, Bandanna Formation, age 254.1+/-0.09 Ma reported here. Calibration of palynological ages. Appears in Fig.15 as having a coal unit shown as Winna.Mbr [=Winnathoola Coal Member] with an age of 254.34 +/- 0.11 Ma.|254.34 +/- 0.11 Ma.||Winna Member.|Overlies Tinowon Formation. Is overlain by Kaloola Member, Bandanna Formation, .|Includes tuff layers.|06-SEP-18
24726|Black Alley Shale|70940|5|Briefly described|p843-845, p850|Permian|Permian|Northern Taroom Trough, central Bowen Basin.||Blackwater Group.||Overlies Tinowon Formation. Is overlain by Kaloola Member.||
24726|Black Alley Shale|71265|5|Briefly described|p587, p589-590, p592, p598-607|Changhsingian|Changhsingian|Bowen and Galilee Basins. Represents a major regional transgression: contains marine sediments. Up to c.20m thick. Sedimentary logs of CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Overlies Peawaddy, Fair Hill Formations. Is overlain by Burngrove Formation. Laterally equivalent to Fair Hill Formation.|Dark shales punctuated with numerous volcanic ash layers.|
24726|Black Alley Shale|71276|5|Briefly described|p285-286, p288, p291-293, p295-298|Lopingian|Lopingian|Mollan et al. (1969); previously the lower part of the Cheshire Formation of Schneeberger (1952) which became the lower Bandanna Formation of Vine et al. (1965). Bowen Basin and western side of Springsure Shelf, Galilee Basin. Pinches out northward in the Bowen Basin, and to the W and E of the Springsure Shelf. Coal seam correlation.||||Overlies Peawaddy and (conformably) Fair Hill Formations. Is overlain by Bandanna, Burngrove Formations, Blackwater Group.||
24726|Black Alley Shale|71701|4|Described|p155-p156, p159, p167-p169, p171|Changhsingian|Wuchiapingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin. Ages are derived from Metcalfe et al, 2015 and are CA-IDTIMS dates; further ages including 254.08 +/- 0.06 Ma are provided.|254.34 +/- 0.08 Ma and 254.10 +/- 0.05 Ma|||Overlies the Peawaddy Formation and the Fair Hill Formation. Overlain by the Bandanna Formation.||
24726|Black Alley Shale|71710|6|Mentioned|p367, 370, 381|||Bowen Basin. Dates of Betts Creek beds equivalents correlated with radiometric ages of this formation.||||Underlain by Peawaddy Formation. Changes laterally to be equivalent to Bandanna Formation.  Deposited during marine transgression, separating Colilea Sandstone and Bandanna Formation.||22-MAY-19
24726|Black Alley Shale|71863|6|Mentioned|p2|Paleozoic|Paleozoic|||||||
24726|Black Alley Shale|72088|4|Described|p8, p20-p21, p38-p40, p91|Changhsingian|Wuchiapingian|Southern Galilee Basin and Bowen Basin.||||Overlies the Peawaddy Formation. Overlain by the Bandanna Formation.|Dark grey to black shale and siltstone with interbedded tuff and sandstone.|
24726|Black Alley Shale|72297|5|Briefly described|p695|||Bowen Basin.||||Correlated with Fair Hill and Burngrove Formations.||
24726|Black Alley Shale|73163|5|Briefly described|p467-468, p472|Lopingian|Lopingian|Both Bowen and Galilee Basins. Date from an ash layer. Deposited during a period of marine transgression. Shown as BAS in Fig. 5, p472. Correlated with younger ash layers in 'Fair Hill Formation equivalent'|254.08 +/- 0.06 Ma CA-IDTIMS.|Betts Creek Group||Overlies the Fair Hill Formation equivalent.|Predominately structureless shale, interbedded with volcanic ash layers.|02-FEB-22
24726|Black Alley Shale|73304|5|Briefly described|p61, p65, p70, p72, p77-78|Changhsingian|Wuchiapingian|Bowen Basin, southern. Age from tuffs. Dating by U-Pb CA-TIMS from near  top and lower part of unit. Middle portion of the unit contains the Wuchiapingian-Changhsingian boundary. Lower portion includes evidence of the top of the P4 glaciation.|254.10 +/- 0.05 Ma, 254.34 +/- 0.08Ma|||||
24726|Black Alley Shale|73305|5|Briefly described|p547-548, p550-p551, p554-556, p560-561|Late Permian|Late Permian|Southern Bowen Basin. Denison Trough, Comet Ridge and northern Taroom Trough. Thins to the north/passes laterally into the laterally equivalent Middle Main Seams. Thickest in the south where the Burngrove Formation wedges out. Varies from 7-120m thickness in southern parts of the basin, thins to the east and north. See also p550, p557 Fig.9. [Misspelt as Black Alley Shale Formation on p547]||||Underlies the Burngrove Formation, stratigraphic equivalent of the Middle Main Seams.|Generally composed of marine mudstone facies, becomes increasingly sandy northwards of the northern Taroom Trough.|12-FEB-23
24726|Black Alley Shale|73472|6|Mentioned|p115-116|Changhsingian|Wuchiapingian|Galilee Basin.||||Underlain by Peawaddy Formation. Overlain by Bandanna Formation. Equivalent to Betts Creek beds.||
24726|Black Alley Shale|73625|5|Briefly described|p1-3, p5 Fig.3, p12, 14-15, 18, 20-21|Permian|Permian|See also p23-26. Bowen Basin. Formed under cold conditions. Graphic sedimentary logs. Hosts rich plant macrofossil assemblages and a diverse marine trace-fossil suite. Changing palaeoenvironments discussed in detail.|c.254.5 - 254 Ma.|||Overlies Peawaddy or Tinowon Formations or Mantuan Productus Bed. Is overlain by Bandanna Formation, Fort Cooper or Baralaba Coal Measures.|Multiple deltaic coarsening-upward cycles. Includes bioturbated mudrocks with interbedded cream-coloured tuffs and/or locally thick coal beds.|
32275|Black Angel Gneiss Complex|64567|4|Described|p1095-1098|Paleoproterozoic|Neoarchean|Replaces Kurbayia Migmatite of Blake (1987). Two suites of orthogneisses. Crystallisation age 2500+/-22 Ma, min age > 1995+/-20Ma (age of Pothole Creek Gneiss).||||||07-NOV-08
32275|Black Angel Gneiss Complex|68307|5|Briefly described|p78, p94|Paleoproterozoic|Paleoproterozoic|North Australian Craton. Part of the basement of the Mount Isa Province. Has strong magmatic arc-like geochemical signature.|?2000-1970 Ma.|||||
32275|Black Angel Gneiss Complex|69591|5|Briefly described|p31|||Mount Isa Province.|~1900-1850 Ma.|Kalkadoon Suite.|||Orthogneiss.|
39016|Black Boy Hill Diorite|23799|5|Briefly described|p63, p65|Late Permian|Early Permian|Age: 270Ma (K/Ar - Willey, 1998).   See also Black Boy Hill diorite and "Black Boy Hill Diorite".  Geological Province: SE Qld. Volcanic and Plutonic Province.||||||
40850|Black Cap Microdiorite|50200|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||
40850|Black Cap Microdiorite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Overlain by Bagstowe Granite. Overlies Old Man Rhyolite.||||||14-MAY-04
40850|Black Cap Microdiorite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province. In Microdiorite Ring Dyke of the Bagstowe Ring Structure.|||||Dark grey porphyritic hornblende-biotite microdiorite.|
40850|Black Cap Microdiorite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Dark grey porphyritic hornblende-biotite microdiorite.|
79369|Black Creek Rhyolite|70740|4|Described|i, iv, p83, p96-p100|||Drummond Basin. Forms a single ignimbrite sheet. Formerly mapped as coherent rhyolite, Bobby Dazzler Rhyolite and volcanic breccia. Is distinguished from the Yacamunda Creek Dacite by larger and more abundant quartz fragments. Named for Black Creek. Outcrop characteristics discussed. A type locality is mentioned but not described. Lithology and petrography is discussed.||Bulgonunna Volcanic Group||Unconformably overlies the Bimurra Volcanics.|Strongly welded, crystal to lithic-rich rhyolitic ignimbrite.|
79369|Black Creek Rhyolite|73035|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|This mapped unit may be shown with some age uncertainty.|||||Light brown-grey, crystal to pumice-rich, strongly welded rhyolitic ignimbrite; medium-coarse fragments of embayed quartz, altered, unzoned plagioclase, alkali feldspar, deformed and altered biotite; abundant felsic volcanic lithics towards base.|
36534|Black Dog basalt|23513|5|Briefly described|Map legend|Silurian|Ordovician|Palaeozoic Volcanic No. V41.||||||
25788|Black Jack Granodiorite|22847|3|Fully described|p 55|Early Devonian|Late Silurian|||||||
25788|Black Jack Granodiorite|42633|5|Briefly described|Table 1 P9|||NOT a variation on Black Jack Formation etc.||||||
25788|Black Jack Granodiorite|42750|2|Defined|p44|Early Devonian|Late Silurian|||||||
25788|Black Jack Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
25788|Black Jack Granodiorite|43259|4|Described|Appendix 1,p50.|Early Devonian|Late Silurian|||||||
25788|Black Jack Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
25788|Black Jack Granodiorite|62521|5|Briefly described|p55|||Of Brittania Supersuite. Geological Province: Ravenswood Batholith. See also Black Jack Granite.||||||14-JAN-08
30125|Black Pinnacle Igneous Complex|22847|3|Fully described|p 58|Permian|Carboniferous|||||||
30125|Black Pinnacle Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Bogie Suite.||||||
30125|Black Pinnacle Igneous Complex|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30125|Black Pinnacle Igneous Complex|43093|4|Described|Appendix 1|Permian|Carboniferous|Reserved as Black Pinnacle Complex.||||||
30125|Black Pinnacle Igneous Complex|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30125|Black Pinnacle Igneous Complex|69593|5|Briefly described|p494-495|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. Commonly associated with intrusives of the Leichhardt Supersuite.|~310-283 Ma.|Bogie Suite.|||Rhyolitic and dacitic ignimbrite; rare andesitic ignimbrite and lava, and andesitic to rhyolitic volcaniclastics. I-type.|
36162|Black Prince Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36162|Black Prince Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36162|Black Prince Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 270. I-Type.||||||
36162|Black Prince Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36162|Black Prince Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Also includes Brownville, Disaster, Glenlinedale, Stingo and Wilderness Granites on most recent maps. Pale pink, med-coarse gr. , porphyritic biotite granite; commonly extensively altered.||||||07-FEB-11
24729|Black Snake Porphyry|22845|6|Mentioned|p54||Triassic|||||||
24729|Black Snake Porphyry|22846|2|Defined|p58-61|Late Triassic|Middle Triassic|Part of the Station Creek Complex.||||||
24729|Black Snake Porphyry|23608|6|Mentioned|p51|||||||||
24729|Black Snake Porphyry|40920|6|Mentioned|p72|||||||||
24729|Black Snake Porphyry|43588|6|Mentioned|p30|Late Triassic|Early Triassic|||||||
24729|Black Snake Porphyry|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
24729|Black Snake Porphyry|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
24729|Black Snake Porphyry|68679|5|Briefly described|p409, p411|Late Triassic|Late Triassic|Northern New England Orogen. A K-Ar (biotite) age of 237.9 +/- 7 Ma (Murphy et al., 1976) is also given.|223 +/- 3 Ma (Lafferty and Golding, 1985).|Station Creek Igneous Complex.|||Quartz diorite to diorite; porphyritic microdiorite.|
27969|Black Soil Andesite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Of the Agate Creek Volcanic Group. Geological Province: Georgetown Region.||||||25-MAY-15
27969|Black Soil Andesite|23430|5|Briefly described|p518|||||||||
27969|Black Soil Andesite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V30.||||||
27969|Black Soil Andesite|43259|4|Described|Appendix 1,p3||Permian|of Agate Creek Volcanic Group.||||||
27969|Black Soil Andesite|43740|4|Described|p30,78||Carboniferous|Includes info on contacts, thickness.||||||01-SEP-04
27969|Black Soil Andesite|50199|5|Briefly described|Map Legend|Early Permian|Early Permian| Agate Creek Volcanic Group.||||||
27969|Black Soil Andesite|50211|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Agate Creek Volcanic Group. Overlain by Thunder Egg Rhyolite. Overlies Talaveras Rhyolite.||||||14-MAY-04
27969|Black Soil Andesite|68353|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Conformably overlies Talaveras Rhyolite. Is overlain conformably by Thunder Egg Rhyolite.|Greyish-green, locally sparsely porphyritic, augite-hypersthene basaltic andesite with agate-filled amygdales; probably includes intrusive equivalents.|
27969|Black Soil Andesite|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province. Has an ancient component of reversely-magnetised remnant magnetisation.||Unit in Agate Creek Volcanic Group.||Conformably overlies Talaveras Rhyolite. Is overlain conformably by Thunder Egg Rhyolite.|Greyish-green, locally sparsely porphyritic, augite-hypersthene basaltic andesite with agate-filled amygdales; probably includes intrusive equivalents; vitric to crystal-rich volcanic lutite and arenite and volcanic rudite.|
27969|Black Soil Andesite|72297|5|Briefly described|p755|||Agate Creek, S of Forsayth. Agates are recovered from decomposed lavas, colluvial deposits and alluvium.||Agate Creek Volcanic Group.|||Amygdaloidal lavas with veins; contains agates.|
24188|Blackeye Granite|23967|6|Mentioned|p1331|||Geological Province: Williams batholith.||||||
24188|Blackeye Granite|24197|5|Briefly described|p96 Tb. 12.1|||Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24188|Blackeye Granite|37862|4|Described|p588|||||||||
24188|Blackeye Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24188|Blackeye Granite|38658|6|Mentioned|p152|||||||||
24188|Blackeye Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24188|Blackeye Granite|39445|6|Mentioned|Table 2|||||||||
24188|Blackeye Granite|40840|6|Mentioned|Map legend|||||||||
24188|Blackeye Granite|41306|6|Mentioned|p4|||||||||
24188|Blackeye Granite|42556|5|Briefly described|Fig.2 P4|||||||||
24188|Blackeye Granite|45161|5|Briefly described|p51|||||||||
24188|Blackeye Granite|45166|5|Briefly described|p38|||||||||
24188|Blackeye Granite|49009|2|Defined|p5|Proterozoic|Proterozoic|Mapped as Williams Granite (Carter & Opik 1963).||||||18-AUG-08
24188|Blackeye Granite|49041|5|Briefly described|Table 3|||||||||
24188|Blackeye Granite|50100|5|Briefly described|p21|Calymmian|Calymmian|Of the Maramungee Suite.||||||
24188|Blackeye Granite|50536|5|Briefly described|p1.5 Table 1.1|||Geological Province: Mount Isa Inlier. Of the Cowie Suite.||||||
24188|Blackeye Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Leucocratic granodiorite, granite, tonalite.||||||
24188|Blackeye Granite|65396|6|Mentioned|p285, p360|||Intrudes the Eastern Succession, Mount Isa Inlier. Syn-post D3 (i.e. <1550 Ma).|~1550 Ma|||||
24188|Blackeye Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Williams Igneous Event||Williams Supersuite|||Pegmatite and leucogranite, commonly foliated; strongly altered|
24188|Blackeye Granite|69591|5|Briefly described|p59|||Maramungee area.|||||Pegmatite and leucogranite, commonly foliated; strongly altered.|
24188|Blackeye Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Cowie Suite|||Pegmatite and leucogranite, commonly foliated; strongly altered.|20-JAN-22
24188|Blackeye Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Of Cowie Suite.|||Pegmatite and leucogranite, commonly foliated and strongly altered.|
28375|Blackheath Sandstone Member|32180|5|Briefly described|p6|||||||||
28375|Blackheath Sandstone Member|38076|6|Mentioned|p26|||||||||
28375|Blackheath Sandstone Member|44510|14|Not recorded|p256|||Member of Blackstone Formation lenticular bed. Useful marker horizon.||||||
28375|Blackheath Sandstone Member|44543|14|Not recorded|p27||Middle Triassic|||||||
27713|Blackman Gap Complex|23291|5|Briefly described|p35|Devonian|Silurian|See also Blackman Gap Supersuite. Of the White Springs Supersuite. Geological Province: Georgetown Region.||||||25-MAR-15
27713|Blackman Gap Complex|23423|5|Briefly described|p263|||||||||
27713|Blackman Gap Complex|23430|5|Briefly described|p486|||Tate Batholith Province||||||
27713|Blackman Gap Complex|23502|5|Briefly described|Map Legend|Early Silurian|Paleoproterozoic|Of White Springs (Blackman Gap) Supersuite. Age: 426+/-7Ma, SHRIMP.||||||07-NOV-08
27713|Blackman Gap Complex|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 340. I-Type.||||||
27713|Blackman Gap Complex|23616|5|Briefly described|Table 1B p11, p29||Silurian|Associated with Blackman Gap Supersuite.||||||11-SEP-08
27713|Blackman Gap Complex|23619|5|Briefly described|p42 Table 2 + p7|||No longer recognised on the Einasleigh Sheet but is recognised in the adjacent Atherton Sheet area.||||||
27713|Blackman Gap Complex|23624|3|Fully described|p5|Early Silurian|Early Silurian|Formerly included in the "Undivided Metamorphics" on 1st. Edition Atherton 1:250 000 geological map.  Age: 426+/-7Ma (U-Pb SHRIMP)||||||
27713|Blackman Gap Complex|23713|6|Mentioned|p11|||||||||
27713|Blackman Gap Complex|41680|3|Fully described|p118|||||||||
27713|Blackman Gap Complex|42054|6|Mentioned|p272|||||||||
27713|Blackman Gap Complex|42691|5|Briefly described|map legend|Precambrian||||||||
27713|Blackman Gap Complex|42765|6|Mentioned|p21|||||||||
27713|Blackman Gap Complex|43060|5|Briefly described|Table 1c|||of Blackman Gap Supersuite||||||
27713|Blackman Gap Complex|43083|5|Briefly described|p115|||Part of Blackman Gap Supersuite.||||||17-JUN-09
27713|Blackman Gap Complex|43087|6|Mentioned|p13|||||||||
27713|Blackman Gap Complex|43110|4|Described|Table 1.|||?Proterozoic and Early Silurian age||||||
27713|Blackman Gap Complex|43113|6|Mentioned|p8|||||||||
27713|Blackman Gap Complex|43259|4|Described|Appendix 1,p40.|Early Devonian|Late Silurian|U-Pb zircon age of 430 Ma. Late Silurian-Early Devonian, possibly some Proterozoic.||||||07-FEB-14
27713|Blackman Gap Complex|43625|6|Mentioned|p18|||Age: 426+/-7 Ma||||||
27713|Blackman Gap Complex|44926|5|Briefly described|Map Legend||Early Silurian|426 +/-7 Ma, SHRIMP||||||
27713|Blackman Gap Complex|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Biotite-muscovite granodiorite and granite.||||||
27713|Blackman Gap Complex|62371|5|Briefly described|p472 Fig.3|Silurian|Silurian|Intrusive rocks.||||||
27713|Blackman Gap Complex|63140|6|Mentioned|p572 Fig.3, p581-582, p583 Fig.13.|Silurian|Silurian|West of and contemporaneous with Hodgkinson Province basalts. Appears as Blackman's Gap Complex on p581, and as Blackmans Gap Complex on p582 and in Fig.13.||||||03-APR-17
27713|Blackman Gap Complex|68330|5|Briefly described|Map legend.|Early Silurian|Early Silurian|Pama Province. Metasedimentary schist and gneiss (Paleoproterozoic) common locally. Altered muscovite-biotite granite to granodiorite mapped separately.|426 +/- 7 Ma (SHRIMP).|Unit in White Springs Supersuite.|||Pale grey to white, medium- to coarse-grained, uneven-grained biotite-muscovite granodiorite and monzogranite; extensively altered in places; minor (muscovite-)biotite granodiorite and monzogranite, pegmatite, aplite, and migmatite.|
27713|Blackman Gap Complex|68331|5|Briefly described|Map legend.|Early Silurian|Early Silurian|Pama Province. Metasedimentary schist and gneiss (Paleoproterozoic) common locally. Altered muscovite-biotite granite to granodiorite mapped separately.|426 +/- 7 Ma (SHRIMP).|Unit in White Springs Supersuite.|||Pale grey to white, medium- to coarse-grained, uneven-grained biotite-muscovite granodiorite and monzogranite; extensively altered in places; minor (muscovite-)biotite granodiorite and monzogranite, pegmatite, aplite, and migmatite.|
27713|Blackman Gap Complex|68405|5|Briefly described|Map Legend|Ludlow|Ludlow|Pama Province. SHRIMP dated.|426 +/- 7 Ma|Of the White Springs Supersuite.||Unconformably overlain by Bulleringa Volcanic Subgroup, Warby Volcanic Subgroup, Sundown Volcanic Group. Older than O'Briens Creek Supersuite, Ootann Supersuite, Claret Creek Supersuite.|Pale grey to cream, variably foliated, medium to coarse-grained, uneven-grained to megacrystic, biotite-muscovite granodiorite, granite; extensively altered in places; minor pegmatite, aplite, schist; metasedimentary pendants and inclusions common.|
27713|Blackman Gap Complex|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Pale grey to cream, variably foliated, medium to coarse-grained, seriate to megacrystic biotite-muscovite granodiorite and granite; extensively altered in places; minor pegmatite aplite, schist; metasedimentary pendants and inclusions common locally.|
27713|Blackman Gap Complex|69592|5|Briefly described|p282, p285|Silurian|Silurian|Shows significant scatter for most elements on Harker-type diagrams; briefly discussed.|426 +/- 7 Ma (SHRIMP U-Pb zircon).|White Springs Supersuite.|||I-type.|
82414|Blacksmiths Creek Monzogranite|71628|5|Briefly described|p12: 1-2, 4-6; p15: 33, 57, 65|||See also p19: 159-160. Name ascribed by Bultitude (unpublished), after a local watercourse. Occurs several kilometres W and NW of Tenterfield. Not adequately mapped. Has an irregular distribution comprising three components (described). Limited geochemistry briefly described.||Sailor Jack Suite.||Intrudes Wallangarra Volcanics and Dundee Rhyodacite (Wandsworth Volcanic Group). Abuts Stanthorpe Complex.|Pale grey, fine-grained, moderately porphyritic hornblende-biotite granodiorite. I-type.|
26398|Blackwall Breccia|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Kholo Subgroup||||
26398|Blackwall Breccia|29386|6|Mentioned|p454|||Upper Triassic.||||||
26398|Blackwall Breccia|30302|6|Mentioned|p415|||Refers Allen(1959)||||||
26398|Blackwall Breccia|30465|5|Briefly described|p3|||||||||
26398|Blackwall Breccia|32180|5|Briefly described|p4|||||||||
26398|Blackwall Breccia|33381|4|Described|p112|||Triassic. See also p117.||||||11-SEP-08
26398|Blackwall Breccia|36779|6|Mentioned|p6|||||||||
26398|Blackwall Breccia|37111|5|Briefly described|p292|||||||||
26398|Blackwall Breccia|38076|6|Mentioned|Table 3|||||||||
26398|Blackwall Breccia|38307|6|Mentioned|p523|||||||||
26398|Blackwall Breccia|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
26398|Blackwall Breccia|39445|6|Mentioned|Table 9|||||||||
26398|Blackwall Breccia|40623|6|Mentioned|Table 2|||||||||
26398|Blackwall Breccia|41906|3|Fully described|Table 2 P19|||||||||
26398|Blackwall Breccia|42336|5|Briefly described|Table 1 P5|||||||||
26398|Blackwall Breccia|43881|14|Not recorded|p134|||Orange card has 'breccia' listed.||||||
26398|Blackwall Breccia|43922|14|Not recorded|p324(map)325|||Formation of Kholo Subgroup, Ipswich Coal Measures.||||||
26398|Blackwall Breccia|44026|14|Not recorded|p122||Triassic|Lithologic equivalent of Neara Volcanics.||||||
26398|Blackwall Breccia|44384|14|Not recorded|p119|||||||||
26398|Blackwall Breccia|44510|2|Defined|p252,Fig.35|||Overlies unconformably the Neranleigh-Fernvale Group from which detritus derived.||||||11-SEP-08
26398|Blackwall Breccia|44542|2|Defined|p32,33,34|||Overlain by Mount Crosby Formation, overlies Weir Basalt.||||||
26398|Blackwall Breccia|44705|14|Not recorded|p1,2,4,9|||||||||
26398|Blackwall Breccia|44734|14|Not recorded|p7|||Pine Mountain area.||||||
26398|Blackwall Breccia|44775|4|Described|p7,8,map 2||Middle Triassic|(Kholo Sub-Group)||||||
26398|Blackwall Breccia|44783|14|Not recorded|p16,18|||||||||
26398|Blackwall Breccia|67402|5|Briefly described|p222, p223|Carnian|Carnian|Ipswich Basin.||Kholo Subgroup||Overlain by the Weir and Sugar Basalts.|Sedimentary breccias.|
26398|Blackwall Breccia|68679|5|Briefly described|pp393-394|Late Triassic|Late Triassic|Locally basal Ipswich Basin. Basal, basement-derived unit. 9m thick in the type section; 30m thick in drill hole.||Basal Kholo Subgroup.||Unconformably overlies Neranleigh-Fernvale beds. Is overlain by and interfingers with Weir Basalt. Is overlain conformably by Mount Crosby Formation.|Matrix-supported granule to pebble sedimentary breccia; massive to poorly bedded, poorly sorted, angular fragments from underlying unit; local conglomerate (slightly rounder clasts); locally contains fragments from Weir Basalt.|
35546|Blackwall Quartz Diorite|23162|5|Briefly described|p882||Early Cretaceous|Age: 132.5+/-2.4Ma. U-Pb SHRIMP zircon dating.||||||19-APR-18
35546|Blackwall Quartz Diorite|69594|5|Briefly described|p567-568, p570, p571 Fig.7.46|Early Cretaceous|Early Cretaceous|Bowen Basin. Geochemistry plots and discussion.|132.5+/- 2.4 Ma (SHRIMP: Allen et al. 1997).|||||
35546|Blackwall Quartz Diorite|70673|6|Mentioned|p128|||Part of a major magmatic event: within uncertainty of the Hecate Granite and Alick Creek Tonalite.|132.5 +/- 2.4 Ma (Allen et al., 1998).|||||
35546|Blackwall Quartz Diorite|71592|5|Briefly described|Appendix A.||||||||Diorite.|
35546|Blackwall Quartz Diorite|73036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Dark greenish grey, medium-grained, moderately porphyritic biotite-hornblende quartz diorite; with accessory titanite and numerous mafic inclusions; commonly partly altered.|
28377|Blackwood Quartz Syenite|40577|3|Fully described|p56|||||||||
28377|Blackwood Quartz Syenite|40954|6|Mentioned|p133|||||||||
28377|Blackwood Quartz Syenite|61917|5|Briefly described|Map legend|Tertiary|Tertiary|Biotite-hornblende-clinopyroxene quartz syenite.||||||
28377|Blackwood Quartz Syenite|65388|4|Described|p420, 421, 422, p403 Fig. 135|Oligocene|Eocene|Of Mount Jukes Intrusive Complex. Younger than Neilson Leucogabbro, older than Jukes Granite. K-Ar ages 34Ma and 33Ma (recalculated) on biotite and alkali feldspar (McDougall & Slessar, 1972). Equigranular, medium grained, greenish grey quartz syenite. Shown as Mount Blackwood Quartz Syenite p421.||||||
28377|Blackwood Quartz Syenite|69599|5|Briefly described|p634|||12 km2.||Mount Jukes Intrusive Complex.|||Equigranular, medium-grained quartz syenite.|
28377|Blackwood Quartz Syenite|73450|4|Described|p45, p71-74|Rupelian|Priabonian|Large mountain-forming stock near Kuttabul. Yielded a U-Pb LA-ICP-MS zircon age of 34.34 +/- 0.7/0.73 Ma (Siegel et al., 2020) and K-Ar ages of 32.6 +/- 1.5 Ma (chloritized biotite) and 33.9 +/- 1.1 Ma (K-feldspar) (McDougall and Slessar, 1972; revised based on Steiger and Jager, 1977).|34.34 +/- 0.7/0.73 Ma U-Pb LA-ICP-MS|Mount Jukes Intrusive Complex|||Equigranular, medium-grained quartz syentie and minor quartz monzodiorite.|
78113|Blantyre Sandstone, Eulo Queen Group|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Eromanga Basin, Carpentaria Basin.||||||
76894|Blaze Creek Gneiss|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event.||Kalkadoon Supersuite|||Broadly layered, pink to cream or grey, porphyritic to equigranular quartzofeldspathic gneiss and subordinate mafic gneiss; local S-C fabrics.|
76894|Blaze Creek Gneiss|68575|4|Described|p1, p6-7, p101-106, p124, p134|||New (tentative) name. Sample area previously mapped as Tewinga Gneiss. Crops out 22km NNE of Dajarra as a rugged N-trending belt up to 5km across. Kalkadoon-Leichhardt Domain, Mount Isa Province. This gneiss represents a phase of the Kalkadoon magmatism (regional basement). Whole rock Sm-Nd isotopic data and age (1858 Ma).|1855 +/- 4 Ma (protolith crystallisation).||||Gneissic granite. Complex intermixtures of medium- to coarse-grained, strongly foliated, felsic and mafic gneisses ranging from massive to strongly porphyritic or porphyroblastic.|17-JAN-17
76894|Blaze Creek Gneiss|69591|5|Briefly described|p60|||Kalkadoon Batholith.|1858 +/- 3 Ma (Magee et al., in press).||||Broadly layered, pink to cream or grey, porphyritic to equigranular quartzofeldspathic gneiss and subordinate mafic gneiss; local S-C fabrics.|
76894|Blaze Creek Gneiss|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain.||||Shown as equivalent to Kalkadoon Granodiorite.|Broadly layered, pink to cream or grey, porphyritic to equigranular quartzofeldspathic gneiss and subordinate mafic gneiss; local S-C fabrics.|
76894|Blaze Creek Gneiss|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain.||||Shown as equivalent to Kalkadoon Granodiorite.|Broadly layered, pink to cream or grey, porphyritic to equigranular quartzofeldspathic gneiss and subordinate mafic gneiss; local S-C fabrics.|
76894|Blaze Creek Gneiss|72919|6|Mentioned|p7|Orosirian|Orosirian|Mount Isa Province. An age of 1855 +/- 4 Ma was reported by Magee et al. (2012).|1855 +/- 4 Ma|||||
76894|Blaze Creek Gneiss|73553|5|Briefly described|p250, p254|Orosirian|Orosirian|Formerly mapped as part of Plum Mountain Gneiss, comprises a discrete north-trending belt ~16.5km west of the main Plum Mountain Gneiss outcrops.|1862+/-3 Ma (Carson et al., 2011)||||Granitic gneiss.|
36492|Blister Swamp complex|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 96.||||||
23394|Blisters Swamp Granite|22847|3|Fully described|p 40|Devonian|Ordovician|||||||
23394|Blisters Swamp Granite|42750|2|Defined|p36|Early Devonian|Middle Ordovician|||||||
23394|Blisters Swamp Granite|43093|4|Described|Appendix 1|Devonian|Ordovician|||||||
23394|Blisters Swamp Granite|43259|4|Described|Appendix 1,p22.|Early Devonian|Ordovician|Middle Ordovician to Early Devonian?||||||
23394|Blisters Swamp Granite|43933|5|Briefly described|Map Legend||Ordovician|||||||
36161|Bloodwood Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||25-JUL-06
36161|Bloodwood Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36161|Bloodwood Granite|60425|4|Described|p191, p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned. Hosts small mica mine where mica is in pegmatite core of a quartz greisen - with books of mica up to 12 cm across. General lithology: pale pink, fine to medium-grained biotite granite; I-type. Included in Sugar Bag Granite on most recent maps.||||||07-FEB-11
36161|Bloodwood Granite|72297|6|Mentioned|p732|Carboniferous|Carboniferous|Muscovite mica was extracted from this unit near Emuford.||||||
80605|Blue Mountains Monzogranite|71792|5|Briefly described|p26|Early Devonian|Early Devonian|[Probably S-type, as part of Kintore Supersuite, which is S-type]||Of Blue Mountains Suite [probably misspelt as Supersuite herein]?|||Biotite monzogranite, hornblende-biotite monzogranite; minor diorite, granodiorite and biotite leucogranite.|
80605|Blue Mountains Monzogranite|71849|4|Described|p4, p8, p17, p20-33, p46, p61, p64, p120|Devonian|Devonian|See also p5, p18, p149, p162-164, p166-168, p173, p179, p184-185, p195. Coen area. Has four informal subunits (mapped separately p8 and described individually in Tb.1 p17-18). Detailed description, geochemistry, photomicrographs. Emplacement at relatively deep crustal levels inferred. Hosts Au-bearing quartz veins; is prospective for intrusion-related gold mineralisation. SHRIMP U-Pb zircon ages by Black et al. (1992).|409 +/- 7 Ma and 405 +/- 13 Ma .|Blue Mountains Supersuite.||Is adjacent to, and may be intruded by, Geikie Granite.|High-K calc-alkaline to shoshonitic, slightly-moderately oxidised, metaluminous-peraluminous granitic rocks. Allanite and titanite are locally conspicuous accessory minerals. Rare epidote of inferred magmatic origin. I-type.|10-APR-19
80605|Blue Mountains Monzogranite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Blue Mountains Supersuite.|||Biotite monzogranite, hornblende-biotite monzogranite; minor diorite, granodiorite and biotite leucogranite.|
80605|Blue Mountains Monzogranite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Five facies variations (lithologies described in the map legend) are mapped separately.||Blue Mountains Supersuite.|||Biotite monzogranite, hornblende-biotite monzogranite; minor diorite, granodiorite and biotite leucogranite.|
80605|Blue Mountains Monzogranite|73387|6|Mentioned|p1, p26, p29|Early Devonian|Early Devonian|Magmatic crystallisation ages of 405 +/- 13 Ma and 409 +/- 7 Ma from Black et al. (1992). Geochemically distinct from Rokeby Quartz Monzodiorite.|405 +/- 13 Ma, 409 +/- 7 Ma SHRIMP zircon|Blue Mountains Supersuite||||20-DEC-22
34858|Blue Mountains Supersuite|22811|6|Mentioned|p603|||of Pama Province||||||
34858|Blue Mountains Supersuite|23420|4|Described|p128, p 147 table 4.6|Early Devonian|Late Silurian|[Age shown in table (40Ma) is in error].  Age (presumably from two plutons in Supersuite)from U-Pb SHRIMP zircons:  405 +/-13 Ma, 409 +/-7 Ma. I-type characteristics.||||||06-DEC-11
34858|Blue Mountains Supersuite|23430|5|Briefly described|p485|||















































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































































||||||06-DEC-11
34858|Blue Mountains Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|This unit, as well as the Flyspeck and Kintore Supersuites, are all mapped under the same symbol, Dg.||||||
34858|Blue Mountains Supersuite|69592|5|Briefly described|p282, p287, p288 Fig.4.84, p289-290,p297|||Cape York Peninsula Batholith. Geochemistry described.|||Blue Mountains, Morris Adamellites.||Hornblende-biotite to biotite-hornblende monzogranite; biotite microgranite; biotite-muscovite granite; hornblende-biotite granodiorite, coarse porphyritic biotite granite; minor pegmatite, aplite. I-type.|
34858|Blue Mountains Supersuite|70207|5|Briefly described|p72|Devonian|Devonian|Northern part of the Cape York Peninsula Batholith. Unit in Pama Igneous Association.|~410-395 Ma.||||I-type.|
34858|Blue Mountains Supersuite|71792|5|Briefly described|p26|Early Devonian|Early Devonian|[probably a misspelling of Blue Mountains Suite because said to be of Kintore Supersuite, in the northern part of the Coen Inlier]|||||Biotite adamellite, hornblende-biotite adamellite, leucocratic biotite granite.|10-AUG-18
34858|Blue Mountains Supersuite|71849|4|Described|p2, p4, p8, p17, p20, p50, p147-149|Devonian|Devonian|See also p151, p162-170, p173-177, p184, p195. Knutson et al. (1994). Coen Inlier. Geochemistry detailed.|||Blue Mountains Monzogranite, Morris Granite, Meldrum Granite.||I-type. Compositions range from metaluminous hornblende-biotite granodiorite to peraluminous biotite-muscovite monzogranite and biotite leucogranite.|
34858|Blue Mountains Supersuite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Blue Mountains Monzogranite, Morris Granite.|||
34858|Blue Mountains Supersuite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Blue Mountains Monzogranite, Meldrum Granite, Morris Granite.|||
34858|Blue Mountains Supersuite|73387|6|Mentioned|p1, p26, p29|||I-type. Previous geochronologic studies noted very few inherited zircons in constituent units.|||Blue Mountains Monzogranite, Morris Granite||Granitoids.|
36549|Blue Range rhyolite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 213.||||||
29431|Blue Rock Creek beds|23291|4|Described|p37, 82 Tb. 3.6|Early Devonian|Early Devonian|First defined by Arnold & Henderson (1976). Max. thickness: 500m. Geological Province: Georgetown Region.||||||08-JUL-15
29431|Blue Rock Creek beds|23431|6|Mentioned|p532|||||||||
29431|Blue Rock Creek beds|23619|4|Described|p33 Table 1||Early Devonian|Also see p8. Underlying unit Halls Reward Metamorphics - unconformably.||||||
29431|Blue Rock Creek beds|42933|4|Described|p220, Fig.71|||Supersedes Blue Rock Creek Beds.||||||
29431|Blue Rock Creek beds|43113|4|Described|Table 1 p20||Early Devonian|||||||
29431|Blue Rock Creek beds|43253|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
29431|Blue Rock Creek beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Broken River Province. This unit, as well as the Shield Creek Formation, Conjuboy Formation and Broken River Group, are all mapped under the symbol, Db.||||||
29431|Blue Rock Creek beds|68731|5|Briefly described|p187, p222, p223 Fig 3.126|Early Devonian|Early Devonian|Arnold and Henderson (1976). A northeasterly trending belt 3 km long and 0.5 km wide. The coral Pseudamplexus and an unpublished conodont determination noted by Withnall (1993) indicate an Early Devonian age for this unit.||||Noncomformably underlain by the Halls Reward Metamorphics.|Consists of recrystallised massive limestone with some calcirudite, micaceous and feldspathic sandstone and shale.|02-JUL-14
29431|Blue Rock Creek beds|69592|6|Mentioned|p228|Middle Devonian|Early Devonian|Comprises remnants of minor basin successions as cover on parts of the North Australian Craton and Thomson Orogen.||||||
36564|Blue St Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 236.  I-Type.||||||
30356|Blue Valley Rhyolite|43259|5|Briefly described|Appendix 1,p7|Early Permian|Late Carboniferous|Of Bulgonunna Volcanic Group||||||
27262|Bluegrass Creek Granite|23161|4|Described|p43,18 table3,5|Early Permian|Late Carboniferous|Ages: 280Ma to 287+/-12 Ma.||||||
27262|Bluegrass Creek Granite|42701|2|Defined|p96, Fig.6 p30|Early Permian|Late Carboniferous|Ages obtained 286Ma, 280Ma K/Ar. see also Blue Grass Creek Granite.||||||
27262|Bluegrass Creek Granite|60659|5|Briefly described|p17, p85|Early Permian|Late Carboniferous|Large composite granodiorite-granite body; red to pink, medium-grained biotite granite is the most extensive rock. Intrudes Locharwood Rhyolite. Age: 286Ma (K-Ar hornblende) and 280Ma (K-Ar biotite).||||||07-FEB-11
27262|Bluegrass Creek Granite|69593|5|Briefly described|p495|Permian|Late Carboniferous|Burdekin Falls Subprovince.|~297-290 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
27262|Bluegrass Creek Granite|70740|5|Briefly described|p83, p122|Permian|Permian|Distribution briefly discussed on p122. K-Ar ages of 286 (Hbl) and 280 (Bt) from Webb and McDougall are mentioned.||||Probably intrudes the Locharwood Rhyolite.|Medium to coarse-grained biotite granite and granodiorite.|
75728|Bluestone Creek Granodiorite|70740|5|Briefly described|p73, p122, p129|||Also referred to as the Bluestone Creek Granite on p73. Distribution and geophysical signature is briefly discussed on p122. Probably also intrudes Bulgonunna Volcanic Group units. Appears to be intruded by Rosetta Creek Granite.||||Intrudes the Bimurra Volcanics.|Light pink to grey, equigranular, medium-grained hornblende, biotite monzogranite to granodiorite with rare hornblende and sphene.|
82990|Bluff Downs Basalt|73115|6|Mentioned|p77|Pliocene|Pliocene|Nulla Basalt Province.|3.63-3.60 Ma|||Overlain by Campaspe Formation.||
81938|Bluff Downs Flow|69789|5|Briefly described|p1042, 1045|Pliocene|Pliocene||3.62 Ma|||Overlies Allingham Formation.|Basalt.|
78909|Boam Creek Quartz Monzodiorite|65388|4|Described|p244-245, p17, 243, 236, 237, 238, 432|Late Carboniferous|Late Carboniferous|Auburn Arch. May have hornfelsed the Torsdale Volcanics. Intruded by Hutchinsons Granite, Mount Appenben Granite and Broadlands Granite. Compared with Lyndale Diorite. Rb-Sr whole-rock isochron age of 311+/- 29 Ma (Webb & McDougall, 1968) of questionable reliability. SHRIMP age: 319+/-5Ma. Mainly green to grey, fine to medium grained hornblende-biotite to biotite quartz monzonite to quartz diorite||||||
78909|Boam Creek Quartz Monzodiorite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.|311 +/- 29 Ma (Rb-Sr: Webb and McDougall, 1968).|||Is intruded by Broadlands, Hutchinsons and Mount Appenben Granites.|Mostly fine- to medium-grained hornblende-biotite quartz monzonite to quartz diorite.|
23396|Boatswain Granodiorite|22847|3|Fully described|p 50|Early Devonian|Late Silurian|||||||
23396|Boatswain Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23396|Boatswain Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23396|Boatswain Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 196. I-Type.||||||
23396|Boatswain Granodiorite|42633|5|Briefly described|Table 1 P8|||Reserved.||||||
23396|Boatswain Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23396|Boatswain Granodiorite|43259|4|Described|Appendix 1,p29.|Early Devonian|Late Silurian|||||||
23396|Boatswain Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23396|Boatswain Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23396|Boatswain Granodiorite|50552|5|Briefly described|p1049 Fig.3|Middle Ordovician|Early Ordovician|In Lolworth-Ravenswood Terrane. Also known informally as Hangingwall Granodiorite. Overlies Footwall Granodiorite, separated by a fault.||||||24-NOV-04
23396|Boatswain Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Boatswain gdrt.||Unit in Millchester Supersuite.||||
23397|Bobby Dazzler Rhyolite|22675|4|Described|p48|Late Carboniferous|Late Carboniferous|Bulgonunna Volcanic Group||||||
23397|Bobby Dazzler Rhyolite|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23397|Bobby Dazzler Rhyolite|23161|4|Described|p17 table3|||||||||
23397|Bobby Dazzler Rhyolite|42701|3|Fully described|p35|||||||||
23397|Bobby Dazzler Rhyolite|43259|6|Mentioned|Appendix 1,p7.|Early Permian|Late Carboniferous|||||||
23397|Bobby Dazzler Rhyolite|43391|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Bulgonuna Volcanic Group. Geological Province: Coastal Ranges Igneous Province.  Grey moderately crysta-rich rhyolitic ignimbrite.||||||23-JUN-04
23397|Bobby Dazzler Rhyolite|44245|5|Briefly described|Map Legend||Carboniferous|||||||
23397|Bobby Dazzler Rhyolite|60659|5|Briefly described|p15|||Part of the Earscliffe association. Moderately crystal- to lithic-rich. Lapilli-ash rhyolitic ignimbrite. Unconformably  overlies Bimurra Volcanics. Of the Bulgonunna Province.||||||07-FEB-11
23397|Bobby Dazzler Rhyolite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
23397|Bobby Dazzler Rhyolite|70740|6|Mentioned|p83, p86-p88, p95|||Distribution briefly discussed on p87. Estimated thickness of 40-60m and no more than 200m maximum.||Bulgonunna Volcanic Group||Overlain by the Locharwood Rhyolite. Probably overlain by the Bungobine Rhyolite. Overlies the Whitestone Creek Dacite.|Moderately crystal-rich, moderately lithic rich, moderately to strongly-welded, lapilli-ash rhyolitic ignimbrite.|
23397|Bobby Dazzler Rhyolite|73035|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Some polygons of this unit are uncertainly identifed.|||||Crystal rich, moderately lithic rich, lapilli-ash dacitic to rhyolitic ignimbrite; rarely developed eutaxitic texture.|
39068|Bobby Volcanics|65452|5|Briefly described|p2-6, p35-36|Late Triassic|Middle Triassic|Southern Yarrol Province. Possibly equivalent to Agnes Water Volcanics: similar geochemistry. Trace elements briefly described. Age based on plant fossils, stratigraphic relationships and correlation with other units.|||||Basal volcaniclastic deposits dominated by clasts of intermediate to mafic lava. Basaltic to andesitic lavas towards top of sequence. Rhyolite and rhyolitic ignimbrite mapped in southern areas.|
39068|Bobby Volcanics|67203|3|Fully described|p1-38, p43-44|Late Triassic|Middle Triassic|Petrology and geochemistry described in detail. At least two different parental magma types. Thickness increases westwards from c.100m to c.600m. SHRIMP U-Pb zircon age from basal airfall deposit. Plant fossils occur in finer-grained sediments. Terrestrial stratovolcano environment. Mafic to intermediate lavas are geochemically similar to those in Bobby Volcanics and Agnes Waters Volcanics: may have formed in one continuous >100km long volcanic field.|229.4 +/- 2.3 Ma (Cross et al., 2009).|||Unconformably overlies Rockhampton Group. Is intruded by Deception Quartz Monzonite, Rule Gabbro and Lawyer Granite. Is correlated with Agnes Water and Mount Marcella Volcanics.|Mafic to intermediate lava flows; fluvial volcaniclastic sediments; pyroclastic deposits; coherent and autoclastic rhyolite in lava domes/cryptodomes.|
39068|Bobby Volcanics|67874|4|Described|p2-3, p13-17, p19, p21, p28, p31, p49|Late Triassic|Middle Triassic|Previously mapped (Dear et al., 1971; Ellis and Whitaker, 1976) as part of Muncon Volcanics. Forms high-relief, densely-vegetated terrain. Shares many similarities with adjacent Agnes Water Volcanics. SHRIMP U-Pb zircon magmatic crystallisation age.|229.4 +/- 2.7 Ma (Cross et al., 2012).|||Unconformably overlies Rockhampton Group.|Basaltic to andesitic lava flows with extensive autoclastic deposits, fluvial volcaniclastic sediments, pyroclastic deposits including ignimbrites and airfall deposits, and coherent autoclastic rhyolite in lava domes/cryptodomes.|
39068|Bobby Volcanics|68008|4|Described|p143, p190-191, p195-199, p214,p329,p416|Middle Triassic|Early Triassic|Many Peaks district. Named after Bobby Range. Subaerial deposits, 250m up to possible 400m thick. Geochemistry described; almost identical to a sample of Native Cat Andesite. Age from plant fossils.||||Overlies Wandilla Formation unconformably, and Bootoo Creek Granite, Miriam Vale Granodiorite and Castletower Granite nonconformably. Is faulted against Nagoorin beds.|Basal volcaniclastic sandstone overlain by massive agglomerate and thick tuff beds, with basalt or basaltic andesite and lapilli tuff at the top. A separate phase in the south contains rhyolite and rhyolitic ignimbrite.|
39068|Bobby Volcanics|68319|5|Briefly described|Map Legend|Late Triassic|Middle Triassic|Poor age control indicated.|||||Greenish brown, hornblende and feldspar-phyric andesite; minor amygdaloidal porphyritic basalt, rhyolite and trachyte; volcanic breccia, mudstone and siltstone, locally with plant remains.|
39068|Bobby Volcanics|68421|5|Briefly described|Map Legend|Late Triassic|Middle Triassic|Triassic Igneous Province.|||||Greenish brown, hornblende and feldspar-phyric andesite; minor amygdaloidal, porphyritic basalt, rhyolite and trachyte; volcanic breccia, mudstone and siltstone, locally with plant remains.|
39068|Bobby Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
39068|Bobby Volcanics|68679|5|Briefly described|p312-313, p434, p436, p442-443|Late Triassic|Late Triassic|Crops out in the Bobby Range to Many Peaks region, northern New England Orogen. Geochemistry and depositional setting suggest a continuous volcanic field with the coeval Agnes Water Volcanics. Petrogenesis involved fractional crystallisation, magma mingling and assimilation. Facies associations described in detail.|229.4 +/- 2.7 Ma (SHRIMP: Cross et al., 2012).|||Unconformably overlies Rockhampton Group.|Thick successions of mafic to intermediate lava flows, commonly with scoriaceous autoclastic domains, locally thick fluvial volcaniclastic intervals, pyroclastics (airfall deposits) and thin ignimbrite interbeds, and rhyolite lava domes/cryptodomes.|
39068|Bobby Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|229+/-2.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
39068|Bobby Volcanics|73450|6|Mentioned|p11, p21|||Interpreted to pre-date Molangul Granite.||||||
38882|Bocoolima Granodiorite|24489|5|Briefly described|Map Legend|Triassic|Permian|Of Galloway Plains Igneous Province.||||||
38882|Bocoolima Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgab].  Deeply weathered grey, medium-grained biotite-hornblende granodiorite.||||||
38882|Bocoolima Granodiorite|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
38882|Bocoolima Granodiorite|68008|2|Defined|p330,p332,p334, p338, p372-375, p380-381|Triassic|Permian|See also p383, p387, p390, p630. New name, after the property Bocoolima. Very deeply weathered and eroded rapidly to form a topographic basin; largely devoid of outcrop. A series of nested plutons, 25 x 15 km. The type area is along the headwaters and tributaries of Bell Creek, S of Blackfellow Mountain. Cut by a later series of NNW-trending andesite dykes. Geophysics described in some detail; part of the Bajool Gravity Low; contrasted with Voewood Granite. Geochemistry detailed; contrasted with Rocky Point Granodiorite and Dumgree Tonalite. No age determination; relative ages from relationships with other units of the Igneous Complex. Geophysics modelled.|Galloway Plains Igneous Complex.|||Intrudes Three Moon, Youlambie Conglomerates, Mount Alma Formation, Rockhampton Group. Is intruded by Voewood Granite, and ?Rocky Point Granodiorite (or vice versa).|Hornblende-biotite granodiorite is virtually the only rock type. Subhedral to euhedral plagioclase laths comprise 50-60% of the rock.|
38882|Bocoolima Granodiorite|68679|5|Briefly described|p424-425, p427|||Yarrol Province. Eastern part of the Complex. Magnetic images suggest two nested plutons. Geochemistry briefly described.||Galloway Plains Igneous Complex.||Intrudes Three Moon and Youlambie Conglomerates, Mount Alma Formation and Rockhampton Group. Is intruded by and surrounds Voewood Granite.|Biotite-hornblende granodiorite.|
33926|Bode syenogranite|22465|6|Mentioned|p935|||Informal name||||||
25798|Bogie Creek Granite|22847|3|Fully described|p 57||Carboniferous|||||||
25798|Bogie Creek Granite|23422|5|Briefly described|p218 Table 6.12|||Of Bogie Suite.||||||
25798|Bogie Creek Granite|23430|5|Briefly described|p495|||Paluma Subprovince. Kennedy Province.||||||
25798|Bogie Creek Granite|23504|5|Briefly described|Map Legend||Carboniferous|||||||
25798|Bogie Creek Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
25798|Bogie Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 116. A?-Type.||||||
25798|Bogie Creek Granite|42245|2|Defined|p40|Middle Carboniferous||Reserved as Bogie Creek Adamallite.||||||11-SEP-08
25798|Bogie Creek Granite|43093|4|Described|Appendix 1||Carboniferous|||||||
25798|Bogie Creek Granite|43259|4|Described|Appendix 1,p23.||Carboniferous|Rb-Sr Biotite age is 311+/-3 Ma.||||||
25798|Bogie Creek Granite|43935|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group?||||||22-FEB-05
25798|Bogie Creek Granite|43936|5|Briefly described|Map Legend||Carboniferous|||||||
25798|Bogie Creek Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Bogie Suite.||||
38250|Bogie Suite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Supersuite.||||||
38250|Bogie Suite|69593|4|Described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|Bogie Creek, Robey Range Granites; Banana Microgranite; Black Pinnacle Igneous Complex.||Biotite and hornblende-biotite granodiorite and granite, microgranodiorite, microgranite, quartz diorite, minor rhyolite.|
34682|Bogie Supersuite|22847|5|Briefly described|p 15|||||||||
24742|Boiler Gully Complex|23032|5|Briefly described|p12|Paleoproterozoic||||||||07-NOV-08
24742|Boiler Gully Complex|23291|4|Described|p30, p20 Fig. 3.2|Early Paleozoic|Proterozoic|Geological Province: Georgetown Region.||||||07-NOV-08
24742|Boiler Gully Complex|23424|6|Mentioned|p330/331|||Structurally identical to Gray Creek Complex.||||||
24742|Boiler Gully Complex|23430|5|Briefly described|p450|||Etheridge Province.||||||
24742|Boiler Gully Complex|23431|5|Briefly described|p531|||Etheridge Province.||||||
24742|Boiler Gully Complex|23494|4|Described|p10, p21 Tb. 1|Devonian|Devonian|Intrudes Hall's Creek Metamorphics and Paddys Creek Formation.||||||
24742|Boiler Gully Complex|23498|6|Mentioned|p21 table 1|||||||||
24742|Boiler Gully Complex|23616|6|Mentioned|Table 1C p16|||Probably equivalent to Sandalwood Serpentinite||||||
24742|Boiler Gully Complex|23619|4|Described|p43 Table 2||Proterozoic|Previously regarded as Devonian. Georgetown Province.||||||
24742|Boiler Gully Complex|29446|4|Described|p122|||||||||
24742|Boiler Gully Complex|30334|6|Mentioned|p120|||||||||
24742|Boiler Gully Complex|30780|5|Briefly described|p996|||||||||
24742|Boiler Gully Complex|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
24742|Boiler Gully Complex|31832|6|Mentioned|Table 6|||||||||
24742|Boiler Gully Complex|31999|6|Mentioned|p139|||||||||
24742|Boiler Gully Complex|32553|4|Described|p66|||||||||
24742|Boiler Gully Complex|32959|6|Mentioned|Fig.30|||||||||
24742|Boiler Gully Complex|35948|6|Mentioned|Table 3|||||||||
24742|Boiler Gully Complex|37570|6|Mentioned|p112|||||||||
24742|Boiler Gully Complex|37571|6|Mentioned|p129|||||||||
24742|Boiler Gully Complex|37575|6|Mentioned|p182|||||||||
24742|Boiler Gully Complex|37768|6|Mentioned|p34|||||||||
24742|Boiler Gully Complex|37769|5|Briefly described|p49|||||||||
24742|Boiler Gully Complex|37770|6|Mentioned|Fig.12|||||||||
24742|Boiler Gully Complex|39027|6|Mentioned|Map legend|Devonian|Devonian|Prob. Devonian||||||
24742|Boiler Gully Complex|39445|5|Briefly described|Table 3|||Greenvale Nickel-cobalt deposit. See also P45, P55 & P56||||||
24742|Boiler Gully Complex|39689|6|Mentioned|p49|||||||||
24742|Boiler Gully Complex|40000|6|Mentioned|p254|||||||||
24742|Boiler Gully Complex|41260|6|Mentioned|p26|||||||||
24742|Boiler Gully Complex|41594|5|Briefly described|p74|||||||||
24742|Boiler Gully Complex|41640|5|Briefly described|p3|||||||||
24742|Boiler Gully Complex|41675|3|Fully described|p17|||||||||
24742|Boiler Gully Complex|41975|5|Briefly described|p439|||||||||
24742|Boiler Gully Complex|42279|6|Mentioned|Fig.2 P18|||||||||
24742|Boiler Gully Complex|42693|5|Briefly described|map legend|Paleozoic|Mesoproterozoic|Age given as Mesoproterozoic to Early Paleozoic.||||||12-DEC-11
24742|Boiler Gully Complex|42747|6|Mentioned|p35|||||||||
24742|Boiler Gully Complex|42752|6|Mentioned|p49|||||||||
24742|Boiler Gully Complex|42933|5|Briefly described|p46|||||||||
24742|Boiler Gully Complex|43060|6|Mentioned|p35|||||||||
24742|Boiler Gully Complex|43113|4|Described|Table 2,p28.||Proterozoic|Ar39-Ar40 minimum ages (Black & others,1979)||||||
24742|Boiler Gully Complex|43213|5|Briefly described|p62|||Eastern Georgetown Province. Mafic-ultramafic. Age uncertain but most likely Mesoproterozoic or Neoproterozoic. Possible correlative of Anakie Metamorphic Group.||||||
24742|Boiler Gully Complex|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
24742|Boiler Gully Complex|43286|5|Briefly described|Map Legend||Proterozoic|||||||
24742|Boiler Gully Complex|43664|6|Mentioned|Fig.3,p15|||||||||
24742|Boiler Gully Complex|43729|5|Briefly described|p3||Proterozoic|||||||
24742|Boiler Gully Complex|44043|14|Not recorded|p69|||||||||
24742|Boiler Gully Complex|44046|14|Not recorded|p152||Early Devonian|Core of serpentinite, mantle of gabbro. Probably early Early Devonian.||||||
24742|Boiler Gully Complex|44048|14|Not recorded|Map Legend||Devonian|||||||
24742|Boiler Gully Complex|44059|14|Not recorded|p442,Table||Early Devonian|Intrudes Paddys Creek Formation. Related to Gray Creek Complex.||||||
24742|Boiler Gully Complex|44258|14|Not recorded|p4||Middle Devonian|(Pre Middle Devonian)||||||
24742|Boiler Gully Complex|44515|2|Defined|p36||Early Devonian|Intrudes Paddys Creek Formation. Related to Gray Creek Complex.||||||
24742|Boiler Gully Complex|45009|2|Defined|p21,27-8,31,41,63,75|||p77,79-87,89,90,107,111-2,130, Pls.11,13,15,Tb.2||||||
24742|Boiler Gully Complex|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|Includes Stenhouse Creek Amphibolite and Sandalwood Serpentinite.||||||07-NOV-08
24742|Boiler Gully Complex|61258|5|Briefly described|p387 Fig. 1|Paleozoic|Neoproterozoic|Geological Province: Georgetown Inlier. Age given as Neoproterozoic to Early Paleozoic.||||||12-DEC-11
24742|Boiler Gully Complex|65887|5|Briefly described|p40 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
24742|Boiler Gully Complex|67455|4|Described|p575 Table 1, p576, p586, pp591-592.|Middle Cambrian|Late Neoproterozoic|Halls Reward domain, Greenvale Province. May represent oceanic crust.|||Includes Sandalwood Serpentinite and Stenhouse Creek Amphibolite.||Interbedded layered amphibolite and metagabbro.|04-MAY-12
24742|Boiler Gully Complex|67848|5|Briefly described|p4.|||Greenvale Province. Mafic-ultramafic assemblage, interleaved with Halls Reward Metamorphics by thrusts.||||||
24742|Boiler Gully Complex|68336|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||Includes Stenhouse Creek Amphibolite and Sandalwood Serpentinite.|||
24742|Boiler Gully Complex|68341|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||Includes Stenhouse Creek Amphibolite and Sandalwood Serpentinite.|||
24742|Boiler Gully Complex|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Cape River Province.|||Includes Sandalwood Serpentinite and Stenhouse Creek Amphibolite.|||04-MAY-15
24742|Boiler Gully Complex|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Greenvale Province. This unit, the Gray Creek Complex, and unnamed mafic and ultramafic intrusive units are all mapped under the same symbol, -P-Cx.||||||
24742|Boiler Gully Complex|68576|5|Briefly described|Q_11: p34-37|||Greenvale area. May represent an early Paleozoic ophiolite. The serpentinite has weathered to form a nickeliferous laterite that was mined in the past (Greenvale Ni-Co deposit) and has been recently re-appraised (details given).|||||Includes amphibolite, metagabbro, clinopyroxenite, serpentinite. Locally mylonitised.|
24742|Boiler Gully Complex|68731|6|Mentioned|p151 Fig 3.51, p156, p158 Fig 3.66|Cambrian|Cambrian||||Includes the Sandalwood Serpentine and the Stenhouse Creek Amphibolite.||Comprises mafic and ultramafic rocks.|
24742|Boiler Gully Complex|69592|5|Briefly described|p250|||Broken River Province. Mafic-ultramafic rocks.||||Intrudes or is tectonically intercalated with Halls Reward Metamorphics.||
31109|Bombarri Granodiorite|23032|5|Briefly described|p39|||||||||
31109|Bombarri Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31109|Bombarri Granodiorite|43480|2|Defined|7,18|Devonian|Silurian|||||||
31109|Bombarri Granodiorite|64707|5|Briefly described|Map legend|Ordovician|Ordovician|Age is probably Orodovician? Foliated grey or pinkish-grey, fine- to medium-gr., subequigranular to locally porph'ic musc/biotite granodiorite, commonly with abundant biotite-rich schleiren and xenoliths of gneiss+amphibolite; cut by pegmatitic stringers.||||||
31109|Bombarri Granodiorite|68338|5|Briefly described|Map legend.|||Unit in Reedy Springs Batholith, Macrossan Province. Age: Ordovician?.|||||Foliated grey or pinkish grey, fine- to medium-grained subequigranular to locally porphyritic muscovite-biotite granodiorite, commonly with abundant biotite-rich schlieren and xenoliths of gneiss and amphibolite and cut by pegmatite stringers.|08-MAY-15
31109|Bombarri Granodiorite|68478|5|Briefly described|Map Legend|Early Silurian|Ordovician|Macrossan Province.|||||Foliated grey or pinkish grey, fine to medium-grained subequigranular to locally porphyritic muscovite-biotite granodiorite, commonly with abundant biotite-rich schlieren and xenoliths of gneiss and amphibolite and cut by pegmatitic stringers.|20-JUN-13
31109|Bombarri Granodiorite|68479|5|Briefly described|Map Legend|Early Silurian|Ordovician|Macrossan Province.|||||Foliated grey or pinkish grey, fine to medium-grained subequigranular to locally porphyritic muscovite-biotite granodiorite, commonly with abundant biotite-rich schlieren and xenoliths of gneiss and amphibolite and cut by pegmatitic stringers.|20-JUN-13
31109|Bombarri Granodiorite|68731|6|Mentioned|p137 Fig 3.22|Ordovician|Ordovician|||||||
31109|Bombarri Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.|410 +/- 6 Ma (SHRIMP U-Pb zircon).|Upland Supersuite.|||I-type.|
37893|Bonnor Suite|23291|4|Described|p96 Tb. 3.11|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
74651|Boodjamulla Formation|67539|5|Briefly described|p14, p15 Fig.8|||Lawn Hill Gorge area. Approximately 300m thick. The upper mudstone cycles contain thin ironstones previously mis-mapped as the Mullera Formation.||Of the South Nicholson Group.||Unconformably overlain by the Constance Sandstone.|Comprises two cycles of sandstone and mudstone.|
74651|Boodjamulla Formation|68575|6|Mentioned|p134|||Whole rock Sm-Nd isotopic data and age (1600 Ma).||||||
74651|Boodjamulla Formation|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1602+/-30 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
80767|Boogaroo Granodiorite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Hornblende granodiorite and diorite to tonalite; minor quartz monzonite, quartz diorite.|
73824|Bookookoorara Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Grey , medium- to fine-grained (marginal zone), moderately to highly porphyritic (titanite-) hornblende-biotite monzogranite; locally granophyric; with mafic inclusions to ~10cm; moderate magnetic response.||||||11-DEC-07
73824|Bookookoorara Monzogranite|63748|6|Mentioned|p36|||Supersedes Bookookoorara Adamellite.||||||07-FEB-11
73824|Bookookoorara Monzogranite|68111|5|Briefly described|p969-972 Figs.2,4, Table 1; p974|Ladinian|Anisian|Large pluton. Dating detailed.|240.1 +/- 2.4 Ma, U-Pb SHRIMP (Li et al. 2012).|||||
73824|Bookookoorara Monzogranite|69639|4|Described|p2, p6, p8-p9, p157-p163, p222, p239|Triassic|Triassic|New England Orogen. Sampling locality, petrography and geochronology are discussed. Geochemically similar to the Bungulla Monzogranite and Undercliffe Falls Monzogranite.|249.8 +/- 1.3 Ma (SHRIMP U-Pb)|Bungulla Suite||Intruded by the Stanthorpe Granite.|Grey-pink, strongly porphyritic biotite monzogranite with a medium-fine grained groundmass.|
73824|Bookookoorara Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Induan|New England Orogen.|249.8 +/-1.3 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
73824|Bookookoorara Monzogranite|71592|5|Briefly described|Appendix A.|||New England Orogen.|250+/-1.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
73824|Bookookoorara Monzogranite|71628|4|Described|p11: 1, 4-7, 14, 36, 45; p15: 33, 52, 57|||See also p15: 62-63, 68; p19: 20-22. Donchak et al. (2007) after Brown et al. (2001). Previously the Bookookoorara Creek body of the Bookookoorara Adamellite (Thomson, 1973, 1976). Named after a local creek. The c.3 x 5 km intrusion occurs ~20 km SE of Stanthorpe. Other age determinations given. Petrology and geochemistry described.|249.8 +/- 1.3 Ma (SHRIMP: Chisholm et al., 2014).|Bookookoorara Suite.||Is bounded by Jenners and Mount Lindesay Monzogranites (Stanthorpe Complex).|Grey, medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite with fine-grained margins; locally granophyric. I-type.|
75128|Boolangalla Granophyre|24613|5|Briefly described|p95, p99|||Flow-banded rhyolite dykes associated with Mount Douglas Formation and Percy Creek Volcanics are probably related to this unit.||||||07-FEB-11
30009|Boolbun Granite|23423|6|Mentioned|p266|||||||||
30009|Boolbun Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30009|Boolbun Granite|43070|2|Defined|p71|Late Permian||Of Cooktown Supersuite.||||||02-JUN-09
30009|Boolbun Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic, (tourmaline)-biotite granite.||||||
30009|Boolbun Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Boolbun Suite (Cooktown Supersuite). Fine- to medium-grained, moderately to highly porphyritic cordierite (altered)-muscovite-biotite granite; accessory zircon, apatite, ilmenite, garnet, tourmaline; intensely deformed in places+mylonitic fabric dev'd||||||07-FEB-11
30009|Boolbun Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Boolbun Suite.|||S-type granitoids.|
69315|Boolbun Suite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains the S-type Boolbun Granite. S-type.||||||07-FEB-11
69315|Boolbun Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Boolbun Granite.||S-type granitoids.|
35036|Boolgal Granophyre|23037|4|Described|92,96||Triassic|Intrudes Coonambula Granodiorite.||||||
35036|Boolgal Granophyre|61087|5|Briefly described|Map Legend|Triassic|Triassic|Pale brown, coarse-grained to aplitic, equigranular, arfvedsonite-bearing leucocratic granophyre.||||||
35036|Boolgal Granophyre|64399|5|Briefly described|Map legend|Triassic|Triassic|Pale brown, coarse-grained to aplitic, equigranular, arfvedsonite-bearing leucocratic granophyre.||||||18-AUG-08
35036|Boolgal Granophyre|65388|1|Redefined|p343-346, 287, 288, p301, 303, 304 |Late Triassic|Late Triassic|Previously defined as Boolgal Granite. Intrudes Nogo beds and surrounding granites of the Rawbelle Batholith, including Coonambula Granodiorite and Culcraigie Granite. Recalculated K-Ar age of 218 Ma (Whitaker & others, 1974). Dominantly pale brown, coarse-grained to aplitic, equigranular, arfvedsonite bearing granophyre. Has characteristics of A-type granites. See also p328, 340, 348.||||||
35036|Boolgal Granophyre|67203|6|Mentioned|p3|Triassic|Triassic|||||||
35036|Boolgal Granophyre|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|This unit, as well as the Greencoat Quartz Monzonite and Mount Saul Quartz Monzonite, are all mapped under the symbol, Rgr.||||||30-SEP-15
35036|Boolgal Granophyre|68679|5|Briefly described|p312, p418-419, p428-429|Late Triassic|Late Triassic|Crops out W of Eidsvold. Northern New England Orogen. This age was recalculated from Whitaker et al. (1974).|218 Ma (K-Ar arfvedsonite).|||Intrudes Culcraigie Granite and Euroka Granodiorite. May intrude Morrow Granite. Adjacent to Mount Eagle Volcanics.|A high-level felsic unit with a well-developed joint system and restricted compositional range. Mainly coarse-grained to aplitic, equigranular, peralkaline, arfvedsonite-bearing miarolitic granophyre. Highly fractionated A-type granite.|
35036|Boolgal Granophyre|73450|4|Described|p10, p23, p26-28, p31, p37|||Connors Province, Auburn Subprovince. [Also written as 'Boolgal Granophyre' to indicate specific usage]. Forms a roughly semi-circular pluton west of Eidsvold with numerous rubbly outcrops. Previously called the Boogal Granite (Whitaker et al., 1974) but renamed by Withnall et al. (2009). Miarolitic cavities and irregular patches/pods of relatively coarse quartz and feldspar ('micropegmatite') are common; crystallised at a relatively high level in the crust. Probably intrudes Mount Eagle Volcanics.||||Intrudes Nogo beds, Morrow Granite, Widbury Granite, and Euroke Granodiorite.|Pale brown, medium-grained, leucocratic granite, typically dominated by alkali feldspar.|
42515|Boomarra Metamorphics|50100|5|Briefly described|p13 Fig. 4|Statherian|Statherian|Geological Province: Eastern Fold Belt.||||||
42515|Boomarra Metamorphics|65387|5|Briefly described|p49|||Stated to be an informal name: ("proposed - IW"). Mount Isa region. Part of a package of undivided gneisses, schists and quartzites of Boomarra Horst, assigned to Soldiers Cap Group.|||||Metasomatised felsic "tuff" layer, hosted by poorly-exposed biotite metapsammite.|
42515|Boomarra Metamorphics|67323|5|Briefly described|p15, p24, p107; GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Eastern Australia Time-Space Plot. Oldest rocks in the eastern Mary Kathleen Domain, Mount Isa Inlier. Erupted during extension of Leichhardt Superbasin. The lower unit of felsic granofels has a similar age to the Argylla Formation. Other, similar, geochronology ages given.|1775 +/- 4 Ma (SHRIMP: OZCHRON).|||Upper (quartzite) part may be equivalent to Ballara Quartzite.|White to pink fine to medium-grained quartzose to feldspathic metasandstone, psammitic schist, minor calc-silicate granofels; common massive to banded amphibolite.|
42515|Boomarra Metamorphics|67539|5|Briefly described|p10|||In Boomarra Horst area. Previously considered Soldiers Cap Group. Divided into three major units. The metasandstone may correlate with the Ballara Quartzite, the felsic granofels with Argylla Formation?||||Probably overlain by Corella Formation.|White, fine-grained, medium to very thick-bedded quartzose metasandstone; pink to grey, felsic granofels; biotite schist and biotite-hornblende granofels with subordinate quartzite.|
42515|Boomarra Metamorphics|68146|5|Briefly described|p127-128, p202|Proterozoic|Proterozoic|Previously mapped as Soldiers Cap Group, which is now known to be much younger (~1690-1650 Ma).|~1785 Ma.|||||
42515|Boomarra Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
42515|Boomarra Metamorphics|68732|6|Mentioned|p165 Fig.3|||In Boomarra Horst. Igneous crystallisation ages.|1777+/-3, 1778+/-3, 1779+/-3 Ma|||||
42515|Boomarra Metamorphics|69056|4|Described|p2-4, p6, p13, p18, p23, p28, p52|Statherian|Statherian|See also Time-Space plot sheet; Reference images sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area. Part of basal cover sequence in the Mary Kathleen and northern Constantine Domains. Poorly exposed. Modelling values listed. Maximum depositional age.|1767 +/- 4 Ma (Neumann et al., 2009).|||Overlies Leichhardt Volcanics, and Argylla Formation possibly conformably. Is overlain by Ballara Quartzite.|Felsic granofels in lower part, overlain by predominantly quartzite.|
42515|Boomarra Metamorphics|69591|4|Described|p29, p34, p57|Paleoproterozoic|Paleoproterozoic|Mary Kathleen Domain. Oldest rocks E of the Pilgrim Fault; unaffected by Barramundi Orogeny. Part of Guide and ?Myally Supersequences. Ages are similar to Argylla Formation. An upper quartzite unit may be equivalent to the Ballara Quartzite.|1776 +/- 8 Ma (Carson et al., 2008).|||Is overlain by Corella Formation. (Probably) equivalent to Argylla Formation.|A lower felsic granofels unit beneath an upper predominantly quartzite unit. White to pink, fine- to medium-grained quartzose to feldspathic metasandstone, psammitic schist, minor calc-silicate granofels; common massive to banded amphibolite.|
42515|Boomarra Metamorphics|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two facies associations are mapped separately.|||||White to pink, quartzose to feldspathic metasandstone and psammitic schist; some pink to grey, hornblende-bearing felsic granofels and minor calc-silicate granofels; common massive to banded amphibolite; rare feldspar-phyric metarhyolite.|
42515|Boomarra Metamorphics|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes two unnamed members; medium grained quartzose -feldspathic metasandstone and biotite-quartz-feldspar schist and minor calc-silicate granofels.|||Includes two unnamed members||Quartzose to feldspathic metasandstone and psammitic schist; some hornblende bearing felsic granofels and minor calc silicate granofels; common massive-banded amphibolite; rare feldspar phyric metarhyolite.|
42515|Boomarra Metamorphics|71592|5|Briefly described|Appendix A.|||Mary Kathleen Domain, Mount Isa Orogen.|1775+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite.|
42515|Boomarra Metamorphics|72596|6|Mentioned|p4|||||||||
42515|Boomarra Metamorphics|72799|6|Mentioned|p1, p4, p26-27, p40|||Intruded by irregular pods of leucogranite, pegmatite and aplite.|||||Includes metasedimentary rocks.|
42515|Boomarra Metamorphics|72889|6|Mentioned|p6 Fig.i.|||||||||
42515|Boomarra Metamorphics|73137|4|Described|p: 1, 5-6, 35, 39, 42, 45-47, 51, 66|Statherian|Statherian|Geochron is a maximum depositional age from a quartzite. Detrital zircon spectra indicate the Kalkadoon-Leichhardt Domain was a prominent source of detritus. Zircon rims yielded a metamorphic age of 1525 +/- 30 Ma. Previous geochron includes a crystallisation age of 1776 +/- 8 Ma from a felsic volcanic rock (Carson et al., 2009) and depositional ages of 1774 +/- 4 Ma and 1775 +/- 4 Ma from felsic volcaniclastic rocks (Page and Sun, 1998). [See article for sampled quartzite field description, petrographic description and detailed geochronology].|1784 +/- 10 Ma|||Equivalent to Argylla Formation.|Includes quartzite and felsic volcaniclastic rocks [and possibly psammitic schist].|
42515|Boomarra Metamorphics|73413|6|Mentioned|App.1|||U-Pb SHRIMP age of 1776 +/- 8 Ma reported by Carson et al. (2008) and 1775 +/- 4 Ma and 1774 +/- 4 Ma by Pase[Page] and Sun (1998).||||||
42515|Boomarra Metamorphics|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mitakoodi-Tommy Creek Domain.|1774+/-4 Ma, 1776+/-8 Ma crystallisation age||||Felsic extrusives, minor mafic extrusives, siliciclastics, carbonaceous clastics.|
42515|Boomarra Metamorphics|73553|4|Described|p8, p20, p29-32, p180,|Statherian|Statherian|Mary Kathleen Domain, far northeast part. Probably equivalent to Argylla Fornation, is equivalent in age to the Argylla Formation but lacks extensive felsic volcanics. Multiple maximum depositional ages provided, 1784+/-10 to 1774+/-4 Ma MDA. Metamorphic age of 1525+/-30 Ma. Previously mapped as Corella Formation or Soldiers Cap Group, much of the Boomanna Horst was assigned to the Boomarra Metamorphics following geochronology studies (Withnall et al., 2016). Known volcanic intervals are included in unnamed subunit 'f', distinguished by slightly higher magnetic responses than the surroundings, and bright whit to greenish tones on radiometric images, other parts have pink to red tones. See also Boonmarra Metamorphics p1. See also p182, p200-201, p203, p205, p207-208.|1776+/-8 Ma U-Pb SHRIMP zircon crystallisation age|||Underlies Corella Formation, intruded by Hillside Bore Granite|Metasedimentary units. Minor felsic volcanics include flow-banded rhyolite, strongly welded pumice-rich ignimbrite.|03-FEB-23
30199|Boomerang Basalt|23291|4|Described|p80 Tb. 3.6|||Of the McBride Basalt Group. Age: 0.23Ma. Geological Province: Georgetown Region.||||||08-JUL-15
30199|Boomerang Basalt|23619|4|Described|p28 table 1||Pleistocene|Olivine basalt. Of the McBride Basalt Group in the McBride Basalt Province.||||||
30199|Boomerang Basalt|43113|4|Described|Table 1 p16||Pleistocene|Of McBride Basalt Group.||||||17-SEP-08
30199|Boomerang Basalt|43253|5|Briefly described|map legend|Quaternary||Of McBride Basalt Group.||||||17-SEP-08
30199|Boomerang Basalt|68576|6|Mentioned|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30199|Boomerang Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pleistocene|Pleistocene|McBride Basalt Province.|0.23 Ma|||||
25801|Boonara Granodiorite|22845|6|Mentioned|p52,54||Triassic|||||||
25801|Boonara Granodiorite|22846|2|Defined|p6,7,61-3|Late Triassic|Middle Triassic|Hosts the Mt Mudlo Copper Mine.||||||
25801|Boonara Granodiorite|24382|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|||||||
25801|Boonara Granodiorite|39505|6|Mentioned|p167|||See also P178.||||||18-AUG-08
25801|Boonara Granodiorite|39997|6|Mentioned|p165|||||||||
25801|Boonara Granodiorite|41738|6|Mentioned|p168|||||||||
25801|Boonara Granodiorite|41778|2|Defined|Table 3|Middle Triassic|Early Triassic|Reserved as Boonara Described P376.||||||18-AUG-08
25801|Boonara Granodiorite|41917|6|Mentioned|p523|||Formerly "Mount Mudlo Granodiorite".||||||18-AUG-08
25801|Boonara Granodiorite|42054|6|Mentioned|p272|||||||||
25801|Boonara Granodiorite|43008|5|Briefly described|map legend|||||||||
25801|Boonara Granodiorite|43588|6|Mentioned|p30|Late Triassic|Early Triassic|||||||
25801|Boonara Granodiorite|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
25801|Boonara Granodiorite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
25801|Boonara Granodiorite|63821|5|Briefly described|p30|Middle Triassic|Early Triassic|Age: 233+/-3Ma (K-Ar). Intrudes Curtis Island Group and Calgoa Diorite; intruded by Boogooramunya Granite. Consists of hornblende (-biotite) granodiorite, porphyritic augite-quartz microdiorite.||||||07-FEB-11
25801|Boonara Granodiorite|68679|5|Briefly described|p332, p428-429|Late Triassic|Late Triassic|Northern New England Orogen. Appears as Boonara Granite on p428.|233 +/- 3 Ma (K-Ar: Cranfield and Murray, 1989).|||Intrudes Neara Volcanics and Calgoa Diorite. Is intruded by Boogooramunya Granite.|Fine- to medium-grained, equigranular biotite-hornblende granodiorite and porphyritic hornblende-pyroxene quartz diorite to diorite.|
27966|Boonmoo Volcanic Subgroup|23291|5|Briefly described|p37|||Parent: Featherbed Volcanic Group. Geological Province: Georgetown Region.||||||26-MAR-15
27966|Boonmoo Volcanic Subgroup|23423|4|Described|p306 Table 7.3||Late Carboniferous|Age: 304 +/- 4 Ma, 306 +/- 3 Ma (Rb-Sr). Intruded by Atlanta, Bamford, Borneo, Gibbs, Hales Siding, Halpin Lass O'Gowrie and Petford Granites.  Featherbed Volcanic Group.||||||
27966|Boonmoo Volcanic Subgroup|23501|6|Mentioned|map legend|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group.||||||
27966|Boonmoo Volcanic Subgroup|23506|5|Briefly described|Map Legend||Late Carboniferous|of Featherbed Volcanic Group.||||||
27966|Boonmoo Volcanic Subgroup|23616|5|Briefly described|Table 3 p48||Carboniferous|Age: 304+/-4 Ma (Rb-Sr). Preserved mainly in Boonmoo "Sag" (Boonmoo and Eight Mile Cauldrons). Intruded by numerous granitoids. Of Featherbed Volcanic Group. Hodgkinson Province.||||||
27966|Boonmoo Volcanic Subgroup|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group.||||||15-JUN-06
27966|Boonmoo Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p9.||Late Carboniferous|||||||
27966|Boonmoo Volcanic Subgroup|43626|4|Described|p10,18||Late Carboniferous|313-301 Ma||||||
27966|Boonmoo Volcanic Subgroup|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27966|Boonmoo Volcanic Subgroup|60425|3|Fully described|p47 and 48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Comprises 11 named subunits. Overlain by Tennyson Volcanic Subgp. Age: 304+/-4Ma and 306+/-3Ma. Intruded by 12 named granites. Thickness: ~2950m in west; ~2000m in east. Ignimbrite, rhyolitic lava - detailed lithology given||||||07-FEB-11
27966|Boonmoo Volcanic Subgroup|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Featherbed Volcanic Group.|Includes Bluewater, Muirson, Hopscotch, Theodolite and Rock Hole Rhyolites; Adder Dacite and Verdure Andesite.|||
27966|Boonmoo Volcanic Subgroup|68576|5|Briefly described|Q_11: p11-12|||Age from constituent (Hopscotch Rhyolite).|c.308 Ma.|Featherbed Volcanic Group.|Muirson, Hopscotch Rhyolites.|||
27966|Boonmoo Volcanic Subgroup|69593|5|Briefly described|p485|Late Carboniferous|Late Carboniferous|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.||||
73902|Boonoo Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Grey to pinkish grey, medium- to fine-grained, slightly to moderately porphyritic muscovite-titanite-biotite monzogranite; with scarce mafic inclusions to ~3cm.||||||11-DEC-07
73902|Boonoo Granite|63748|4|Described|p35-36|||Of the Boonoo Suite. Referred to as the "Spring Creek body" of the Bookookoorara Adamellite by Thomson (1976). Grey to pinkish grey, fine- to medium-grained, porphyritic (hornblende-titanite-) biotite monzogranite, with scattered feldspar.||||||07-FEB-11
73902|Boonoo Granite|68111|5|Briefly described|p969, p970 Fig.2, p971, p972 Fig.4, p974|Anisian|Olenekian|Dating detailed.|245.6 +/- 2.5 Ma, U-Pb SHRIMP (Li et al. 2012).|Of the Herries Supersuite.||||
73902|Boonoo Granite|69639|5|Briefly described|p44, p74, p217, p220|Anisian|Anisian|New England Orogen.|245.6 +/- 2.5 Ma  (SHRIMP U-Pb, Li et al, 2012)|Herries Supersuite||||
73902|Boonoo Granite|70876|5|Briefly described|p80-p81|Early Triassic|Early Triassic|Provided age is a SHRIMP U-Pb zircon date.|245.6 +/- 2.5 Ma (Li et al, 2012)|Herries Supersuite||||
73902|Boonoo Granite|71628|6|Mentioned|p11:4|||Donchak et al. (2007).||||||
82369|Boonoo Monzogranite|71628|3|Fully described|p19: 20-22; p15: 33, 52, 57, 62, 77|||See also p11: 4-6, 36. New name (this study), after the Boonoo State Forest. Originally the Spring Creek body of Bookookoorara Adamellite of Thomson (1973, 1976); later the Boonoo Granite of Donchak et al. (2007). Forms ~3 x 1 km intrusion about 10 km NNW of Tenterfield. Crops out as scattered, sometimes large, rounded boulders. The type locality is roadside outcrops along the Mount Lindesay Highway (Donchak et al., 2007). Geochemistry described.|245.69 +/- 2.5 Ma (SHRIMP: Li et al., 2012).|Boonoo Suite.||Abuts The Ram Swamp Monzogranite and is enclosed by Mount Lindesay Monzogranite (Stanthorpe Complex); probably intruded by them.|Grey to pinkish grey, medium- to fine-grained, weakly to moderately porphyritic biotite-(amphibole) monzogranite. I-type.|
73903|Boonoo Suite|63748|5|Briefly described|p35-36|||Of Herries Supersuite. Includes Boonoo Granite.||||||07-FEB-11
73903|Boonoo Suite|71628|6|Mentioned|p19: 21||||||Boonoo Monzogranite.|||
39860|Boorama Tank Gneiss|24254|5|Briefly described|p24|Proterozoic|Proterozoic|Age: 1545 +/- 11 Ma (U/Pb).||||||
39860|Boorama Tank Gneiss|60665|6|Mentioned|p1157 Fig.9. |Calymmian|Calymmian|Southern Cloncurry intrusion. Age inferred from Fig.9.|1547 +/- 6 Ma.|||||
39860|Boorama Tank Gneiss|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Age: 1550-1540 Ma.||||||
39860|Boorama Tank Gneiss|63866|5|Briefly described|p64||||1547 +/- 5 Ma (Page and Sun, 1998)|||||
39860|Boorama Tank Gneiss|64250|6|Mentioned|p11 fig 3|||Cloncurry Fold Belt, Mount Isa Inlier.|1547 +/- 5 Ma|||||
39860|Boorama Tank Gneiss|65396|6|Mentioned|p7, p56, p82, p84, p157, p175, p241|Calymmian|Calymmian|Cloncurry Fold Belt. Eastern succession.|1547 +/- 5 Ma (SHRIMP: Page and Sun, 1998)|||||
39860|Boorama Tank Gneiss|65755|5|Briefly described|p13|||1555 Ma||||||
39860|Boorama Tank Gneiss|66913|5|Briefly described|p171 fig 2|Calymmian|Calymmian|U-Pb zircon SHRIMP age shown diagramatically on Fig. 2.||||||
39860|Boorama Tank Gneiss|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p21|||See also references to the (superseded) Boorama Tank gneiss (GIS attrib tbl; p21).|1547 +/- 5 Ma (Page and Sun, 1998).|?Cowie Suite.||||
39860|Boorama Tank Gneiss|69591|5|Briefly described|p59|||Maramungee area.|1547 +/- 5 Ma (Page and Sun, 1998).||||Medium-grained, weakly- to strongly-foliated gneissic granite.|
39860|Boorama Tank Gneiss|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Cowie Suite.|||Medium-grained, weakly to strongly foliated gneissic granite.|05-MAY-16
39860|Boorama Tank Gneiss|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Cowie Suite.|||Medium grained, weakly to strongly foliated gneissic granite.|
39860|Boorama Tank Gneiss|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1547+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)|||||
39860|Boorama Tank Gneiss|72949|6|Mentioned|p35|Calymmian|Calymmian|Mount Isa Inlier, Western Fold Belt.||||||
39860|Boorama Tank Gneiss|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1547 +/- 5 Ma|||||
25802|Boori Igneous Complex|22847|3|Fully described|p 59|Early Permian|Carboniferous|||||||
25802|Boori Igneous Complex|23083|6|Mentioned|p683|||||||||
25802|Boori Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Tuckers Suite.||||||
25802|Boori Igneous Complex|23504|5|Briefly described|Map Legend||Permian|||||||
25802|Boori Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 194. I-Type.||||||11-AUG-15
25802|Boori Igneous Complex|23617|5|Briefly described|p30|||||||||
25802|Boori Igneous Complex|30148|4|Described|p29|||Upper Carboniferous - Lower Permian age.||||||
25802|Boori Igneous Complex|30149|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous to Lower Permian.||||||
25802|Boori Igneous Complex|30151|4|Described|Table 2|||Upper Carboniferous - Lower Permian age.277-282 m.y.||||||
25802|Boori Igneous Complex|30914|6|Mentioned|Map legend|Permian|Permian|||||||
25802|Boori Igneous Complex|31813|6|Mentioned|Table 2|||Carb. - Permian||||||
25802|Boori Igneous Complex|32553|4|Described|p58|||||||||
25802|Boori Igneous Complex|34409|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous - Lower Permian||||||
25802|Boori Igneous Complex|34573|6|Mentioned|p31|||280my. See p37.||||||11-AUG-15
25802|Boori Igneous Complex|36472|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Early Permian to Late Carboniferous||||||
25802|Boori Igneous Complex|37613|6|Mentioned|Fig.3|||||||||
25802|Boori Igneous Complex|39445|5|Briefly described|Table 12|||||||||
25802|Boori Igneous Complex|39734|6|Mentioned|p21|||||||||
25802|Boori Igneous Complex|41668|5|Briefly described|p12|||||||||
25802|Boori Igneous Complex|42245|6|Mentioned|p36|||||||||
25802|Boori Igneous Complex|43093|4|Described|Appendix 1|||K-Ar date of 284+/-9Ma.||||||
25802|Boori Igneous Complex|43259|4|Described|Appendix 1,p29.|Permian|Carboniferous|K-Ar age is 280+/-8 Ma. Carboniferous? to Permian.||||||
25802|Boori Igneous Complex|43936|5|Briefly described|Map Legend||Permian|||||||
25802|Boori Igneous Complex|45151|5|Briefly described|Table 7|||||||||
25802|Boori Igneous Complex|48914|2|Defined|p82|Permian|Carboniferous|Carb. - Perm.||||||
25802|Boori Igneous Complex|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Tuckers Suite.||||
36250|Boot Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36250|Boot Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 283. I-Type.||||||
36250|Boot Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36250|Boot Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Fine-grained, granophyric biotite granite; also includes Boulder Peak granite on most recent maps.||||||07-FEB-11
70426|Bootoo Creek Granite|65452|6|Mentioned|p6 Fig.2|||||||||
70426|Bootoo Creek Granite|67203|6|Mentioned|p6|Permian|Late Carboniferous|||||||
70426|Bootoo Creek Granite|68008|6|Mentioned|p199|||||||Is overlain nonconformably by Bobby Volcanics.||
70426|Bootoo Creek Granite|68421|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||Intrudes the Duckpond Road Metamorphics.|Foliated pale pink porphyritic biotite granite and microgranite.|
70426|Bootoo Creek Granite|68679|5|Briefly described|p404, p409|||Wandilla Province. Possibly Carboniferous-Permian.|||||Foliated, porphyritic biotite granite and microgranite.|
70426|Bootoo Creek Granite|73450|6|Mentioned|p21|||Interpreted to pre-date Molangul Granite.||||||
37010|Booyal Surface|23251|5|Briefly described|p2, p26|||Named by Cranfield (1994). occur to the west of the Como Scarp. An indurated landscape. Geological Provicne:  Maryborough Basin.||||||21-JUN-06
37010|Booyal Surface|63821|4|Described|p11|||Forms red, indurated soil profile; developed on Tawah Granite at Brant Bridge; formed on Tert. seds.E. of Barambah Ck; an undulating erosion surface developed on undivided Duckinwilla Group in SE corner of MARYBOROUGH sheet; overlain by Elliott Surface.||||||07-FEB-11
41797|Bora Creek Quartz Monzodiorite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Grey to pinkish grey, medium grained biotite hornblende quartz monzodiorite and subordinate granite.||||||
41797|Bora Creek Quartz Monzodiorite|61035|4|Described|p7, p10 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Broadsound Volcanics and unconformably overlain by Leura Volcanics. Age: 314+/-3Ma and 331+/-5Ma (M. Fanning, SHRIMP). Biotie-hornblende quartz monzodiorite and hornblende-biotite granite. Geol Prov: Connors Sudprovince.||||||07-FEB-11
41797|Bora Creek Quartz Monzodiorite|65388|2|Defined|p353-354, p86, 90 , 95, 361, 393, 399|Late Carboniferous|Late Carboniferous|Connors Arch pluton. Intrudes Broadsound Range Volcanics/Rhyolite. Overlain by Leura Volcanics. SHRIMP age 316.4+/- 2.6 Ma on 12 zircon grains (MSWD = 0.54). Second population gives 329+/-5 Ma suggesting inherited component, but more work needs to be done. Mainly pinkish grey to grey, medium grained, equigranular biotite-hornblende quartz monzodiorite. Also Bora Creek Monzodiorite on p393.||||||
41797|Bora Creek Quartz Monzodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus,Toobier, Tooloombah Creek and Waitara Granites; the Clement Creek Quartz Monzodiorite; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
41797|Bora Creek Quartz Monzodiorite|68679|5|Briefly described|p347, p356, p362|Pennsylvanian|Pennsylvanian|Southern Connors Subprovince, northern New England Orogen. Age determination and inherited zircons discussed on p362.|316.4 +/- 3.4 Ma (SHRIMP: Fanning et al., 2009).|||Intrudes the Broadsound Range Volcanics. Is overlain nonconformably by Leura Volcanics.||
41797|Bora Creek Quartz Monzodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Monzodiorite.|
39066|Borilla Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
39066|Borilla Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pale pink, medium-grained, seriate, granophyric syenogranite commonly with small miarolitic cavities generally with quartz and K-feldspar infill.|
39066|Borilla Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Age based on similarities with other dated granites.|||||Pale pink, medium-grained, seriate, granophyric syenogranite commonly miarolitic. A-type; peraluminous but not peralkaline.|
39066|Borilla Granite|73450|4|Described|p10, p16, p22-23, p28, p31, p37|late Triassic|late Triassic|A-type. Comprises a stock with a northerly elongation. Previously mapped as part of the Miriam Vale Granodiorite (Ellis, 1974). Contains numerous small (up to ca 1 cm across), irregular miarolitic cavities or irregular pegmatitic patches/pods. Crystallised under relatively low pressures at high level in the crust. Not yet radioisotopically dated although it is most probably late Triassic. Interpreted to post-date the adjacent Cassilis Granite, Conella Granodiorite, Gaeta Diorite, and Thornhill Gabbro. It is cut by very few dykes, if any.|||||Pale pink, fine- to medium-grained, somewhat uneven grained, very leucocratic alkali feldspar granite.|
30421|Borneo Granite|23423|6|Mentioned|p306 Table 7.3|||||||||
30421|Borneo Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 304+/-4 Ma, Rb-Sr. of Ootann Supersuite.||||||
30421|Borneo Granite|23616|6|Mentioned|Table 3 p48|||||||||
30421|Borneo Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite). Pale grey to pink, abundantly porphyritic (hornblende-)biotite microgranite; grey, fine biotite granite. Age: 304+/-4Ma.||||||26-MAR-15
30421|Borneo Granite|43567|5|Briefly described|Table 2,p401|||||||||
30421|Borneo Granite|43626|6|Mentioned|p11|||||||||
30421|Borneo Granite|60425|6|Mentioned|p49 Tb.3|||Informal name - see Borneo Granodiorite. Intruded Boonmoo Volcanic Subgroup.||||||07-FEB-11
30421|Borneo Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Both of these variants have a geophysical subdivision. All four sub-units are mapped separately.|304 +/- 11 Ma (Rb-Sr, whole rock).|Unit in Ootann Supersuite.|||Grey, highly porphyritic hornblende-biotite microgranodiorite; pale grey to pink, highly porphyritic (hornblende-)biotite microgranite, grey, fine-grained biotite granite.|
30421|Borneo Granite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.|Ootann Supersuite.||||
39072|Bororen Tonalite|65452|6|Mentioned|p6 Fig.2|Permian|Permian|||||||
39072|Bororen Tonalite|67203|6|Mentioned|p6-7, p31|Permian|Permian|West and southwest Bobby Range area.||||||
39072|Bororen Tonalite|68008|4|Described|p324, p326, p413-414, p416|Triassic|Permian|Various outcrops are listed. Named after the small township of Bororen. Appears to have been separated from the geophysically distinct Miriam Vale Granodiorite. Deeply weathered; forms low topography. Geophysics briefly described.||||Is surrounded by (intrudes) the Miriam Vale Granodiorite and Jackass Gabbro.|The surface expression is a granitic soil (grus). Original rock type was a biotite tonalite. Remnants of foliation still visible.|
39072|Bororen Tonalite|68319|5|Briefly described|Map Legend|Permian|Permian||||||Pale brown to brown, medium-grained biotite tonalite; extensively weathered, decomposed; locally deformed and partly recrystallised.|
39072|Bororen Tonalite|68421|5|Briefly described|Map Legend|Permian|Permian||||||Pale brown to brown, medium-grained biotite tonalite; extensively weathered, decomposed; locally deformed and partly recrystallised.|
39072|Bororen Tonalite|68679|5|Briefly described|p421, p423|||Gayndah-Gladstone belt.|||||Pale brown, biotite tonalite; locally deformed and partly recrystallised.|
28307|Boroston Formation|23032|4|Described|p33||Tournaisian|||||||
28307|Boroston Formation|23424|4|Described|Table 8.1 p337.||Early Carboniferous|Age: Early Carboniferous (Tournaisian); superposition. Intruded by Montgomery Range Igneous Complex. Lithologically equiv to upper part of Venetia Fm. Of Bundock Creek Gp, Bundock Basin. Max thickness ~850 m.||||||
28307|Boroston Formation|23430|5|Briefly described|Plate 14.11 + p510||Carboniferous|Also see p507. Of Bundock Creek Group. Graveyard Creek Subprovince.||||||
28307|Boroston Formation|23431|5|Briefly described|p541|||||||||
28307|Boroston Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Visean|Visean|Of the Bundock Creek Group. Overlain by the Harry Creek Formation. Overlies the Teddy Mountain Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
28307|Boroston Formation|24613|5|Briefly described|p135|||In the upper part of the Bundock Creek Group. Geological province: Broken River Province.||||||07-FEB-11
28307|Boroston Formation|24614|5|Briefly described|p191 Fig. 1|||Geological Province: Broken River Province.||||||07-FEB-11
28307|Boroston Formation|41260|3|Fully described|p94|||||||||
28307|Boroston Formation|41679|6|Mentioned|Fig.2|||||||||
28307|Boroston Formation|41719|6|Mentioned|Fig.2|||||||||
28307|Boroston Formation|41739|2|Defined|p304|early Tournaisian||||||||
28307|Boroston Formation|41740|6|Mentioned|p222|||||||||
28307|Boroston Formation|42054|6|Mentioned|p273|||||||||
28307|Boroston Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
28307|Boroston Formation|42709|6|Mentioned|map legend|||||||||
28307|Boroston Formation|42933|3|Fully described|p171|||of Bundock Creek Group||||||
28307|Boroston Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bundock Creek Group.||||||
28307|Boroston Formation|43603|5|Briefly described|p9|||||||||
28307|Boroston Formation|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Bundock Creek Group. Map symbol  (Co) implies that unit considered entirely Carboniferous.||||||28-AUG-14
28307|Boroston Formation|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group. Micaceous, lithofeldspathic sublabile sandstone, conglomerate and mudstone; minor siltstone and reworked tuff; quartzose sandstone and conglomerate towards base.||||||
28307|Boroston Formation|67402|4|Described|p239, p245 |Tournaisian|Tournaisian|Bundock Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under alluvial fan, alluvial plain or lacustrine conditions. Maximum thickness of 850m. ||||Overlies the Teddy Mount Formation. Overlain by the Harry Creek Formation.|Quartzose to lithofeldspathic sandstone, conglomerate and mudstone; minor siltstone and reworked tuff.|
28307|Boroston Formation|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Micaceous, lithofeldspathic sublabile sandstone, conglomerate and mudstone; minor siltstone and reworked tuff; quartzose sandstone and conglomerate towards base.|
28307|Boroston Formation|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Micaceous, lithofeldspathic sublabile sandstone, conglomerate and mudstone; minor siltstone and reworked tuff; quartzose sandstone and conglomerate towards base.|
28307|Boroston Formation|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Micaceous, lithofeldspathic sublabile sandstone, conglomerate and mudstone; minor siltstone and reworked tuff; quartzose sandstone and conglomerate towards base.|
28307|Boroston Formation|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Harry Creek Formation. Conformably underlain by the Teddy Mount Formation.|Micaceous, lithofeldspathic sublabile sandstone, conglomerate and mudstone, and minor siltstone and reworked tuff; quartzose sandstone and conglomerate towards base.|
28307|Boroston Formation|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Bundock Basin (Broken River Province).||Bundock Creek Group.||||
28307|Boroston Formation|69592|4|Described|p272 Fig.4.61, p273-274, p276|Tournaisian|Tournaisian|Bundock Basin, Broken River Province. Up to 850m thick in the NW, thinning to <100m in the SE. Sediment source was a crystalline basement (the Georgetown Inlier) with significant volcaniclastic input in the upper part. Alluvial fan deposits. Only fossils are indeterminate plant remains. Probable age is constrained by underlying Teddy Mount Formation.||Bundock Creek Group.||Conformably overlies Teddy Mount Formation. Is overlain conformably by Harry Creek Formation.|Medium-grained to very coarse-grained, cross-bedded sandstone, pebbly sandstone and granule to cobble conglomerate. Sandstones are lithofeldspathic to quartzose, and commonly micaceous.|
81002|Bottom Seam|68679|6|Mentioned|p398|Late Triassic|Late Triassic|Informal subdivision of the coal measures (Reid 1945, 1947; Dear, McKellar & Tucker 1971; Flood 1985) recognised a basal conglomerate followed above by the Bottom, Sawmill, Callide and Marker seams.||Callide Coal Measures.||||30-APR-19
36249|Boulder Peak Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36249|Boulder Peak Granite|60425|4|Described|p285 Appdx., p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Medium- to coarse-grained, porphyritic biotite granite; I-type. Included in Boot Granite on most recent maps. Informally referred to as Sandy granite also.||||||07-FEB-11
68959|Bourgamba Microgranite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Roaring Meg Suite (Cooktown Supersuite). S-type. Mainly fine- to med- grained, even-grained to slightly porphyritic, (altered cordierite?-) tourmaline-biotite-muscovite granite; minor greisen.||||||07-FEB-11
68959|Bourgamba Microgranite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Roaring Meg Suite.|||S-type granitoids.|
23413|Bousey Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Wirra Volcanic Subgroup. Age: 325+/-7Ma (Black & Holmes, unpub.ms.) Thickness: Up to 900m. Geological Province: Georgetown Region.||||||28-MAY-15
23413|Bousey Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V22. I-Type.||||||
23413|Bousey Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23413|Bousey Rhyolite|40542|6|Mentioned|p97|||||||||
23413|Bousey Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Wirra Volcanic Subgroup.||||||
23413|Bousey Rhyolite|43740|4|Described|p7|||||||||
23413|Bousey Rhyolite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Wirra Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
23413|Bousey Rhyolite|50199|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Wirra Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
23413|Bousey Rhyolite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Nine facies are mapped separately.||Unit in Wirra Volcanic Subgroup.|||Crystal-rich rhyolitic ignimbrite; volcanic breccia; volcanic lutite to arenite; aphyric rhyolite lava, airfall tuff, minor volcaniclastic sediment and breccia; rare limestone.|
23413|Bousey Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Wirra Volcanic Subgroup.|||Grey to green or brown and purple rhyolitic volcanic lutite to volcanic rudite; rare limestone.|
23413|Bousey Rhyolite|69593|5|Briefly described|p512|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|330 Ma.|Newcastle Range Volcaniuc Group.|||I-type.|
23413|Bousey Rhyolite|70207|5|Briefly described|p82||||323.4 +/- 3.5 Ma (SHRIMP zircon: Black, 1998).|Basal Wirra Volcanic Subgroup.||||
23413|Bousey Rhyolite|71592|5|Briefly described|Appendix A.||||323+/-3.5 Ma (SHRIMP U-Pb zircon).||||Ignimbrite.|
28393|Bowarrady dune sand|38302|6|Mentioned|Table 1|||Informal name||||||
28393|Bowarrady dune sand|39495|6|Mentioned|p142|||||||||
28393|Bowarrady dune sand|62102|5|Briefly described|p367 Tb. 1, p371|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast.  Age: 263Ka.||||||09-MAY-06
75123|Bowden granite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal.Of the Bedarra Suite (Bedarra Batholith or Supersuite?) in Bedarra Granite Belt. Mainly pale grey to pale brown, medium-grained, moderately porphyritic biotite granite+biotite-rich schlieren/zones; I-type; cut by microgranite dykes/quartz veins.||||||07-FEB-11
39613|Bowler Creek Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Porphyritic biotite granite.||||||01-JUL-04
39613|Bowler Creek Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, medium- to coarse-grained, porphyritic biotite granite.|
39613|Bowler Creek Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith. Large elliptical plutons (mostly 20-75 km2).||Forsayth Supersuite.|||Megacrystic granite.|
24196|Bowlers Hole Granite|24197|5|Briefly described|p27, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Argylla Suite. Intrusive rocks. Age: 1780Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24196|Bowlers Hole Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24196|Bowlers Hole Granite|37862|4|Described|p585|||||||||
24196|Bowlers Hole Granite|38350|4|Described|p17|||||||||
24196|Bowlers Hole Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24196|Bowlers Hole Granite|38658|6|Mentioned|p152|||||||||
24196|Bowlers Hole Granite|39445|5|Briefly described|Table 2|||||||||
24196|Bowlers Hole Granite|40840|6|Mentioned|Map legend|||||||||
24196|Bowlers Hole Granite|41978|6|Mentioned|p501|||||||||
24196|Bowlers Hole Granite|45161|5|Briefly described|p31|||See also p19.||||||02-APR-07
24196|Bowlers Hole Granite|45166|5|Briefly described|p34|||||||||
24196|Bowlers Hole Granite|49009|2|Defined|p8|Proterozoic|Proterozoic|Mapped as Kalkadoon Granite (Carter & Opik 1963).||||||02-APR-07
24196|Bowlers Hole Granite|49041|5|Briefly described|Table 2|||||||||
24196|Bowlers Hole Granite|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Of the Argylla Formation into which it intrudes.  Geological Province: Kalkadoon-Ewen Province / Eastern Fold Belt.||||||02-APR-07
24196|Bowlers Hole Granite|50536|5|Briefly described|p1.4, 4.2 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Argylla Suite.||||||07-NOV-08
24196|Bowlers Hole Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite-hornblende granite.||||||
24196|Bowlers Hole Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Kalkadoon Igneous Event.||Kalkadoon Supersuite.||Intrudes Argylla Formation.|Foliated biotite-hornblende granite, gneissic-granite.|
24196|Bowlers Hole Granite|67497|6|Mentioned|p909|Statherian|Statherian||~1780 Ma|Of the Argylla Suite|||A-type granite|
24196|Bowlers Hole Granite|69591|5|Briefly described|p60|||Wonga Batholith.|||||Foliated biotite-hornblende granite, gneissic granite.|
24196|Bowlers Hole Granite|72596|5|Briefly described|p1-3, p46, p49-55|Statherian|Statherian|Crops out on the western side of the Fountain Range Fault. Geochronologic constraint is a magmatic crystallisation age from 28 constituent analyses. This age is generally within accepted range (ca. 1775-1780 Ma) for the Argylla Magmatic Event of Neumann et al. (2009).|1777 +/- 4 Ma SHRIMP U-Pb|Argylla Suite.||Comagmatic with Argylla Formation. Intrudes Magna Lynn Metabasalt and Leichhardt Volcanics.|Amphibolite-grade metamorphosed[?] granite.|19-JAN-22
24196|Bowlers Hole Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Foliated biotite-hornblende granite, gneissic -granite.|
24196|Bowlers Hole Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Foliated biotite-hornblende granite, gneissic -granite.|
24196|Bowlers Hole Granite|73137|6|Mentioned|p90|Statherian|Statherian||1777 +/- 4 Ma|||||
24196|Bowlers Hole Granite|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb age of 1777 +/- 4 Ma reported by Kositcin et al. (2019).|1777 +/- 4 Ma|||||
24196|Bowlers Hole Granite|73525|6|Mentioned|p4-5 Fig.2, p17, p19 Fig.13|||Kalkadoon-Leichhardt Domain. Undated.|||||Felsic intrusive.|
24196|Bowlers Hole Granite|73553|4|Described|p2, p8, p15, p18, p27-28,|Statherian|Statherian|Mary Kathleen Domain. Argylla Igneous Province, comagmatic with Argylla Formation. Ovoid pluton with north-trending elongation. Mottled pink tones on radiometric images, low magnetic response. Cut by numerous dolerite (now metadolerite, amphibolite) dykes and scattered quartz veins. Subalkaline, metaluminous geochemistry, mainly oxidised and shoshonitic. A-type. Assigned to Argylla Suite by Budd et al., (2001). Contains a distinct core of fractionated biotite granite. See also p2, p8 Fig.1.2.3, p15, p53, p62-63, p80, p36-39, p42-46, p53, p63-64, p80, p246-249.|1777+/-4 Ma U-Pb zircon SHRIMP|Argylla Suite||Intrudes Argylla Formation, Magna Lynn Metabasalt, Leichhardt Volcanics|Pale pinkish brown to pinkish grey, fine- to medium-grained biotite-amphibole granite, amphibole-biotite granite, and minor biotite granite, moderately-strongly developed foliation. Extensively recrystallised.|03-FEB-23
80377|Bowthorn Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). Marine shelf unit.||Constance Sandstone.||Overlies Shultz Sandstone Member. Is overlain unconformably by Elizabeth Sandstone.||
80377|Bowthorn Member|71369|4|Described|p1, p6-7, p12, p23-24, p28, p32-36,|Mesoproterozoic|Mesoproterozoic|See also p49-50. Originally the Bowthorn Siltstone Member of Slater and Mond (1980), Sweet et al. (1981). It was abandoned as a Member of the Constance Sandstone, and absorbed into the Schultz Sandstone Member, by Rawlings et al. (2008). Resurrected and modified in this study as Bowthorn Member (Sweet, 2017) to apply to the upper part of the Constance Sandstone. The type section is 4-5km south of Bowthorn homestead in an area of very low dips and is estimated to be about 300m thick there South Nicholson Basin. Up to 400m thick. A series of prograding marine sand bodies.||Constance Sandstone.||Overlies Schultz Sandstone Member. Is overlain unconformably by Elizabeth Sandstone.|Coarsening-up sequences of green laminated shale, interbedded siltstone and very fine sandstone, to fine sandstone with scattered glauconite.|20-FEB-18
80377|Bowthorn Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72526|5|Briefly described|p8 Fig.1.3, p33, p34.|Mesoproterozoic|Mesoproterozoic|Shown as located in the central and eastern parts of the South Nicholson Basin.||Constance Sandstone||Overlies and is laterally equivalent to Constance Sandstone and underlies Mullera Formation.||
80377|Bowthorn Member|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin.||Constance Sandstone||Part equivalent to Mittebah Sandstone and underlies Mullera Formation.||
80377|Bowthorn Member|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the central part of the South Nicholson Basin.||Upper part of Constance Sandstone.||Laterally equivalent to Mittebah Sandstone. Underlies Mullera Formation.|Includes dolomitic siltstone.|
80377|Bowthorn Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Underlain by and partly equivalent to Constance Sandstone. Overlain by Mullera Formation.||
80377|Bowthorn Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Unconformably overlain by Elizabeth Sandstone[?].||
25807|Box Forest Quartz Diorite|22847|3|Fully described|p 52|||||||||
25807|Box Forest Quartz Diorite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
25807|Box Forest Quartz Diorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 123.||||||
25807|Box Forest Quartz Diorite|42245|2|Defined|p35|Early Devonian||Reserved as Box Forest Quartz-Diorite||||||
25807|Box Forest Quartz Diorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
25807|Box Forest Quartz Diorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Late Silurian to Early Devonian?.||||||
25807|Box Forest Quartz Diorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Box Forest qtz-drt.||||||
27116|Boxwell Granodiorite|42748|2|Defined|p6|Late Triassic|Late Permian|||||||
27116|Boxwell Granodiorite|63733|5|Briefly described|Map legend|Late Permian|Late Permian|Pale to dark grey or pinkish grey, medium- to fine-grained biotite-hornblende and hornblende-biotite granodiorite; minor monzodiorite-quartz monzodiorite, monzogranite, syenogranite; high magnetic response.||||||11-DEC-07
27116|Boxwell Granodiorite|63748|4|Described|p32|Late Permian|Early Permian|Of Boxwell Suite. Mascotte granodiorite (Shaw 1981). Intrudes Texas beds. Age: 255-252Ma (Rb-Sr biotite). Compositionally zoned with monzodiorite-qtz monzodiorite margin grading inwards to granodiorite and core of monzogranite + leucocratic syenogranite||||||07-FEB-11
27116|Boxwell Granodiorite|65668|6|Mentioned|p1|Permian|Permian|Texas area. Age: ~ 257 Ma.||||||
27116|Boxwell Granodiorite|68003|5|Briefly described|p31, p32 Fig.3-h, p131.|Late Permian|Late Permian|Central Block, New England Fold Belt. I-type. Also called Boxwell Creek Granodiorite on p31.||Unit in Clarence River Suite.|||Dark grey, medium- to coarse-grained, equigranular, hornblende-bearing monzodiorite and quartz monzodiorite.|
27116|Boxwell Granodiorite|68005|5|Briefly described|p63, p135.|Early Permian|Early Permian|||Unit in Clarence River Supersuite.|||Dark grey, medium- to coarse-grained, equigranular, hornblende-bearing monzodiorite and quartz monzodiorite.|
27116|Boxwell Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Jibbinbar, Mount Bullaganang, Mount You You and Palgrave Granites, and Greymare Granodiorite, are all mapped under the symbol, Pgn.||||||
27116|Boxwell Granodiorite|68679|4|Described|p455-457, p464-465|Permian|Permian|Northern New England Batholith. Crops out mainly in NSW. ~22 km2. A zoned pluton with a margin of monzodiorite to quartz monzodiorite grading into granodiorite, and a core of monzogranite and leucocratic syenogranite. Generally strongly oxidised, moderately-highly evolved, low-medium-K, I-type. Geochemistry briefly described: geochemical plots; similar to Dumbudgery Creek Granodiorite.|256.6 +/- 1.7 Ma (SHRIMP: Cross and Blevin, 2010).|Boxwell Suite.||Intrudes Texas beds.|Grey or pinkish-grey, fine- to medium-grained porphyritic (pyroxene-)hornblende-biotite and biotite-hornblende granodiorite to quartz monzodiorite; accessory titanite, allanite; rarely miarolitic.|
27116|Boxwell Granodiorite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
27116|Boxwell Granodiorite|70036|5|Briefly described|Map legend|Permian|Permian|New England Fold Belt.|||||Includes granodiorite.|
27116|Boxwell Granodiorite|70217|5|Briefly described|v, p73 tbl 14.1 , p74|Wuchiapingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from Cross and Blevin (2010). |256.6 +/- 1.7 Ma (SHRIMP U-Pb)|Boxwell Suite||||
27116|Boxwell Granodiorite|70876|5|Briefly described|p78|Permian|Permian|SHRIMP date is derived from Cross and Blevin, 2010. [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|256.6 +/- 1.7 Ma (SHRIMP U-Pb zircon)|Boxwell Suite||||
27116|Boxwell Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|257+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
27116|Boxwell Granodiorite|71628|4|Described|p9: 1-2; p10: 1-10; p19: 103, 158|||Stroud (1992). Included in Clarence River Supersuite by Bryant et al. (2003) after unpublished work by Chappell and Bryant (1994). Removed to Boxwell Suite within Boxwell Supersuite by Donchak et al. (2007) on locational and geochemical grounds. Named after a local island in the Dumaresq River. Crops out ~10 km W of Texas, as boulders in undulating country. Mostly covered by alluvium. A zoned pluton; petrology and geochemistry detailed. I-type.|256.6 +/- 1.7 Ma (Cross and Blevin, 2010).|Boxwell Suite.||Intrudes Texas beds.|Dark grey, medium- to coarse-grained, equigranular quartz monzodiorite (margin), medium-grained, slightly porphyritic hornblende-biotite granodiorite (dominant), and light pink, locally porphyritic, monzogranite to leucocratic syenogranite (core).|
69438|Boxwell Suite|63748|5|Briefly described|p32|Late Permian|Early Permian|Of the Boxwell Supersuite. Includes Boxwell Granodiorite.||||||07-FEB-11
69438|Boxwell Suite|68679|5|Briefly described|p457, p465|Permian|Permian|Northern New England Batholith; mostly in NSW.|~256 Ma.|Clarence River Supersuite.|Boxwell Granodiorite.|||
69438|Boxwell Suite|70217|5|Briefly described|p32|||New England Orogen. ||Boxwell Supersuite|Includes the Rocky Creek Granodiorite and the Boxwell Granodiorite.|||
69438|Boxwell Suite|70876|5|Briefly described|p80|Permian|Permian|Age derived from SHRIMP dates for the constituent Boxwell Granodiorite and Rocky Creek Granodiorite.||Clarence River Supersuite|Includes the Boxwell Granodiorite and Rocky Creek Granodiorite.|||
69438|Boxwell Suite|71628|5|Briefly described|p5: 1; p9:2; p10: 1, 3, 5, 9, 11|||Donchak et al. (2007) after unpublished work by Blevin (ca. 2004). Redefined in this study as a Supersuite.||Boxwell Supersuite.|Boxwell Granodiorite.|||
69437|Boxwell Supersuite|63748|5|Briefly described|p32|Late Permian|Early Permian|Includes the Boxwell Suite.||||||07-FEB-11
69437|Boxwell Supersuite|70217|5|Briefly described|v, p73 tbl 14.1, p74|Permian|Permian|Includes 4 I type granodiorites in the Northwest New England Orogen. Is geochemically similar to the Clarence River Supersuite. |||Includes the Boxwell Granodiorite and the Rocky Creek Granodiorite.|||
69437|Boxwell Supersuite|71628|5|Briefly described|p9:2; p10: 1-11; p19: 157-158|Late Permian|Late Permian|Donchak et al. (2007); redefined in this study. Comprises a handful of more sodic intrusives in the NW portion of the Southern New England Orogen. Geochemistry summarised and contrasted with other Supersuites.|||Apple Tree Gully, Boxwell, Dry Creek, Kings Plains Suites.||Quartz monzodiorite, granodiorite (dominant) and monzogranite.|
26421|Bracker Sandstone|30914|6|Mentioned|Map legend|Permian|Carboniferous|Devonian  - Permian||||||
26421|Bracker Sandstone|31587|6|Mentioned|p59|||Geological map||||||
26421|Bracker Sandstone|44543|2|Defined|p30||Permian|Overlies unconformably Beacon Mudstone.||||||
26421|Bracker Sandstone|44565|2|Defined|p230-232|||Fresh water. On NSW and QLD cards.||||||
26421|Bracker Sandstone|44786|14|Not recorded|p193-202||Permian|||||||
26421|Bracker Sandstone|48940|6|Mentioned|Fig.14|||Refers Lucas (1959,1960)||||||
24760|Bracteata Mudstone|23032|5|Briefly described|p27 fig6|Devonian|Devonian|||||||
24760|Bracteata Mudstone|23424|5|Briefly described|Table 8.1 p335|Givetian|Emsian|Of Wando Vale Subgroup/Broken River Group, Graveyard Creek Subprovince.||||||
24760|Bracteata Mudstone|41260|4|Described|p159|||Reserved as Bracteata Creek Mudstone. See also Table 1||||||
24760|Bracteata Mudstone|41679|2|Defined|p258|late Emsian||||||||
24760|Bracteata Mudstone|41719|6|Mentioned|Fig.2|||||||||
24760|Bracteata Mudstone|41739|6|Mentioned|Fig.2|||||||||
24760|Bracteata Mudstone|41740|6|Mentioned|p222|||||||||
24760|Bracteata Mudstone|42031|5|Briefly described|Fig.5 P762|||||||||
24760|Bracteata Mudstone|42054|6|Mentioned|p273|||||||||
24760|Bracteata Mudstone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
24760|Bracteata Mudstone|42933|3|Fully described|Table 2|||See also p102||||||
24760|Bracteata Mudstone|65214|6|Mentioned|p272|Devonian|Devonian|QLD NORTH. Appears as Bracteata Formation on p272. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
24760|Bracteata Mudstone|68336|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Mudstone with lesser, very fine- to medium-grained, calcareous, lithofeldspathic arenite and minor nodular, lenticular limestone.|
24760|Bracteata Mudstone|68341|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Mudstone with lesser, very fine- to medium-grained, calcareous, lithofeldspathic arenite and minor nodular, lenticular limestone.|
24760|Bracteata Mudstone|68478|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Mudstone with lesser, very fine to medium-grained, calcareous, lithofeldspathic arenite and minor nodular, lenticular limestone.|
24760|Bracteata Mudstone|68479|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Mudstone with lesser, very fine to medium-grained, calcareous, lithofeldspathic arenite and minor nodular, lenticular limestone.|
24760|Bracteata Mudstone|69592|4|Described|p259, p264-266|Emsian|Emsian|Wade Anticlinorium; southern Graveyard Creek Subprovince, Broken River Province. Up to 170m thick; wedges out northwards. Paralic, later shallow muddy shelf, deposits. Age from macrofossils.||Basal Wandovale Subgroup.||Overlies Shield Creek Formation. Is overlain conformably by Lomandra Limestone or Storm Hill Sandstone.|Massive to laminated, bioturbated mudstone interlayered with subordinate thin-bedded, fine-grained, calcareous sandstone; interbeds of diversely fossiliferous limestone in the upper part.|
26294|Brae Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26294|Brae Formation|36925|2|Defined|p183|Early Permian|Early Permian|||||||
26294|Brae Formation|38204|4|Described|p74|||||||||
26294|Brae Formation|38310|6|Mentioned|p237|||||||||
26294|Brae Formation|38917|6|Mentioned|p168|||||||||
26294|Brae Formation|40091|5|Briefly described|p72|||||||||
26294|Brae Formation|40093|4|Described|p30|||||||||
26294|Brae Formation|41246|6|Mentioned|Map legend|Permian||||||||
26294|Brae Formation|41546|6|Mentioned|p157|||||||||
26294|Brae Formation|41666|6|Mentioned|p15|||See also Fig.1||||||
26294|Brae Formation|43017|5|Briefly described|Fig.3,p375|||||||||
26294|Brae Formation|64856|5|Briefly described|p48|||Overlies Buffel Formation where locally developed.| | ||||31-JAN-13
26294|Brae Formation|65388|5|Briefly described|p160, 165, 166, 167|||These rocks included in the Oxtrack Formation in this study. Of Back Creek Group, Bowen Basin. Of Flood & others (1981),  Briggs (1993). Disconformable over Buffel Formation. Conformably overlain by Oxtrack Formation. Younger than Buffel Formation. Regarded by Draper (pers. comm., 2000) as part of Oxtrack Formation. Status of this unit not resolved in this study.||||||
26294|Brae Formation|68679|5|Briefly described|p378|||Flood et al. (1981). Bowen Basin. 160m thick. Marine shelf deposits.|||||Mudstone, siltstone, fossiliferous sandstone.|
78910|Brae Member|65388|5|Briefly described|p160, 162||Artinskian|Listed here as of Buffel Formation but probably better considered part of the Oxtrack Formation. Discontinuous outcrop. ~160m of typically well-laminated green to buff mudstone and interbeds of strongly bioturbated sandstone.||||||
27723|Branch Creek Formation|30451|4|Described|p31|||At base of Boiling Creek Group. Upper Carboniferous.||||||
27723|Branch Creek Formation|31659|6|Mentioned|p58|Namurian|Namurian|In Yarrol district.||||||09-JUN-09
27723|Branch Creek Formation|32141|6|Mentioned|p152|||||||||
27723|Branch Creek Formation|32867|6|Mentioned|p74|||See also p21.||||||
27723|Branch Creek Formation|32868|6|Mentioned|p200|||||||||
27723|Branch Creek Formation|33728|6|Mentioned|p50|||||||||
27723|Branch Creek Formation|33774|6|Mentioned|p23|||Refers Maxwell (1959)||||||
27723|Branch Creek Formation|33992|6|Mentioned|p238|||M.Carb.  See also p239||||||
27723|Branch Creek Formation|34085|6|Mentioned|Cor.chart|||Westphalian||||||
27723|Branch Creek Formation|35492|6|Mentioned|p145|||||||||
27723|Branch Creek Formation|36528|6|Mentioned|p174|||||||||
27723|Branch Creek Formation|39445|5|Briefly described|Table 7 p98|||||||||
27723|Branch Creek Formation|39632|6|Mentioned|p224|||||||||
27723|Branch Creek Formation|42547|4|Described|p52|||||||||
27723|Branch Creek Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
27723|Branch Creek Formation|43983|14|Not recorded|p1-5,8,9,12,14|||||||||
27723|Branch Creek Formation|43992|14|Not recorded|p197||Westphalian|4 miles east of Dakiel.||||||
27723|Branch Creek Formation|44091|14|Not recorded|p37,Tb.3,p47||Early Carboniferous|||||||
27723|Branch Creek Formation|44360|2|Defined|p1-3,14-7,21-8,30-34||Westphalian|Map. Unit of Boiling Creek Group. (Middle Westphalian)||||||
27723|Branch Creek Formation|44369|2|Defined|p169-171|||Subgreywacke, chert, conglomerate.||||||
27723|Branch Creek Formation|44370|14|Not recorded|Tb.7,p219|||||||||
27723|Branch Creek Formation|44372|6|Mentioned|p5-7||Namurian|Overlies Baywulla Formation. Underlies Poperima Formation.||||||
27723|Branch Creek Formation|44379|14|Not recorded|p15|||Ref. to Dear J.F. unpublished PhD Thesis 1963.||||||
27723|Branch Creek Formation|44515|2|Defined|p29,30|||||||||
27723|Branch Creek Formation|44833|14|Not recorded|p120|||Early Carboniferous faunal zones.||||||
27723|Branch Creek Formation|44874|14|Not recorded|p102|||||||||
27723|Branch Creek Formation|45097|6|Mentioned|Fig.|||Carboniferous correlation chart||||||
27723|Branch Creek Formation|68008|5|Briefly described|p120|Late Carboniferous|Late Carboniferous|Maxwell (1959, 1960, 1964). Yarrol and Cannindah areas. Subsequently subsumed into the Lorray Formation.||Boiling Creek Group.||||
27723|Branch Creek Formation|68679|5|Briefly described|p341|||Maxwell (1959). Cannindah area. Superseded; assigned to Boiling Creek Group by McKellar (1967) which itself is (?being) replaced by Lorray Formation.||Boiling Creek Group.||||
36237|Branch Creek Rhyolite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Gingerella Cauldron Complex, Sundown Volcanic Group.||||||
36237|Branch Creek Rhyolite|23624|4|Described|p22|Permian|Carboniferous|Intrudes the Blackman Gap Complex.||||||08-JUL-15
36237|Branch Creek Rhyolite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gingerella Cauldron Complex.|||Porphyritic microgranite, flow-banded intrusive rhyolite and breccia containing coarse clasts of rhyolite and granite.|
36237|Branch Creek Rhyolite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gingerella Cauldron Complex.|||Porphyritic microgranite, flow-banded intrusive rhyolite and breccia containing coarse clasts of rhyolite and granite.|
23415|Brandy Hot Granodiorite|23291|4|Described|p90 Fig. 3.8|Silurian|Silurian|See also Brandy Hot Granite. Parent: Brandy Hot Supersuite. Age: Silurian? Geological Province: Georgetown Region.||||||24-JUN-15
23415|Brandy Hot Granodiorite|23513|5|Briefly described|Map legend||Silurian|Palaeozoic Intrusive No. 64. I-Type.||||||
23415|Brandy Hot Granodiorite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23415|Brandy Hot Granodiorite|40542|6|Mentioned|p97|||                    ite||||||
23415|Brandy Hot Granodiorite|41272|5|Briefly described|M 1of1 E04|||||||||
23415|Brandy Hot Granodiorite|43259|4|Described|Appendix 1,p19.|Early Devonian|Late Silurian|Age based on gamma-ray spectrometrics signature.||||||
23415|Brandy Hot Granodiorite|50595|5|Briefly described|Map Legend|Silurian|Silurian|Porphyritic muscovite-biotite granodiorite.||||||01-JUL-04
23415|Brandy Hot Granodiorite|67341|5|Briefly described|p57-59|Calymmian|Calymmian|Etheridge Province. Crops out ~20km W of Georgetown. Classified in a separate Supersuite because its chemistry and gamma-ray spectrometric signature are distinctly different from surrounding granites. Magmatic crystallisation age.|1563 +/- 3 Ma (SHRIMP U-Pb zircon).|Brandy Hot Supersuite.||Intrudes Etheridge Group.|Felsic, porphyritic muscovite-biotite granodiorite. I-type.|
23415|Brandy Hot Granodiorite|68352|5|Briefly described|Map legend.|||Pama Province. Max Age: Silurian? Min Age: Silurian?|||||Grey, medium- to coarse-grained, sparsely-porphyritic muscovite-biotite granodiorite with 10-15 mm pink K-feldspar phenocrysts.|18-MAY-15
23415|Brandy Hot Granodiorite|69591|5|Briefly described|p82|Mesoproterozoic|Mesoproterozoic|Occurs on the W side of the Forsayth Batholith, 20km W of Georgetown. Chemically and radiometrically distinct from the surrounding Forsayth Supersuite granites. Previously thought to be Silurian, and treated as the sole member of the Brandy Hot Supersuite [!]. Later shown to be Mesoproterozoic and coeval with Forest Home Trondhjemite; probably best assigned to the Forest Home Supersuite.|1563 +/- 3 Ma (Neumann and Kositcin, 2011).|||Intrudes Etheridge Group.|Felsic, I-type, porphyritic muscovite-biotite granodiorite.|
23415|Brandy Hot Granodiorite|69592|5|Briefly described|p284|Mesoproterozoic|Mesoproterozoic|Bain et al. (1997); Withnall et al. (2002). A unit in the Pama Igneous Association. Prior to the age determination by Neumann and Kositcin, this was the sole constituent of the Brandy Hot Supersuite.|~1560 Ma (SHRIMP U-Pb: Neumann and Kositcin, 2011)|Forest Home Supersuite.||||
23415|Brandy Hot Granodiorite|73642|5|Briefly described|p4 Tb.1|Calymmian|Calymmian|Georgetown Inlier.|1563+/-6 Ma|Forrest Home Supersuite||||
75732|Brawl Creek Granite|70740|5|Briefly described|p118, p122, p126|||Distribution and outcrop described briefly on p122. Probably intrudes the Bulgonunna Volcanic Group.||||Probably intrudes the Bulgonunna Volcanic Group. Probably intruded by Glenmore Creek Granite.|Pale pink, mainly medium-grained, slightly porphyritic, granophyric leucocratic biotite monzogranite with rare hornblende and sphene.|
27724|Breakaway Shale|22836|6|Mentioned|Fig.10 p402|||||||||
27724|Breakaway Shale|23031|5|Briefly described|26|||Geol province Leichardt River Subprovince. Parent Mount Isa Group. Overlying unit Native Bee Siltstone, underlying unit Moondara Siltstone.||||||17-DEC-07
27724|Breakaway Shale|23363|5|Briefly described|356|Statherian|Statherian|1663+/-3Ma||||||
27724|Breakaway Shale|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group.||||||07-NOV-08
27724|Breakaway Shale|23397|5|Briefly described|p467 Fig.2|Statherian|Statherian|1663+/-3Ma||||||
27724|Breakaway Shale|23398|5|Briefly described|p455|Statherian|Statherian|of Mount Isa Group.  1663+/-3Ma||||||
27724|Breakaway Shale|23399|4|Described|p494|Statherian|Statherian|Of Mount Isa Group, 1663+/-3Ma.||||||01-OCT-08
27724|Breakaway Shale|23408|5|Briefly described|p511, 512, p513 Fig. 2|||Prominent marker horizon in the Mount Isa Group. Contains the Breakaway Chert towards the top.||||||15-JUN-09
27724|Breakaway Shale|23466|5|Briefly described|p269|||||||||
27724|Breakaway Shale|23518|4|Described|p12|Proterozoic|Proterozoic|Of Mount Isa Group.  Geological Province: Western Fold Belt.||||||
27724|Breakaway Shale|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Mount Isa Group||||||15-JUN-09
27724|Breakaway Shale|24419|5|Briefly described|p17, p18|Paleoproterozoic|Paleoproterozoic|The predominant siliceous siltstone and shale are leached in outcrop but are carbonaceous at depth.  Conformably overlies Moondarra Siltstone; conformably overlain by Native Bee Siltstone. Part of the Gun Supersequence.||||||07-NOV-08
27724|Breakaway Shale|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of Mount Isa Group. Overlies Moondarra Siltstone. Age: 1663 Ma. Geological Province: Leichardt River Trough.||||||
27724|Breakaway Shale|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group.  Overlies the Moondarra Siltstone; underlies the Native Bee Siltstone.||||||25-AUG-04
27724|Breakaway Shale|30535|6|Mentioned|p403|||See also P405. Refers Bennett(1965) and type section||||||
27724|Breakaway Shale|31207|6|Mentioned|Table 1|||||||||
27724|Breakaway Shale|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27724|Breakaway Shale|32041|4|Described|p355|||||||||
27724|Breakaway Shale|32042|5|Briefly described|p39|||||||||
27724|Breakaway Shale|32376|6|Mentioned|Table 3|||||||||
27724|Breakaway Shale|32660|5|Briefly described|Table 5|||||||||
27724|Breakaway Shale|32959|6|Mentioned|Fig.21|||||||||
27724|Breakaway Shale|33900|5|Briefly described|p14|||||||||
27724|Breakaway Shale|34499|6|Mentioned|Table 1|||||||||
27724|Breakaway Shale|35074|6|Mentioned|Fig.2|||||||||
27724|Breakaway Shale|35116|6|Mentioned|Table.4|||||||||
27724|Breakaway Shale|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27724|Breakaway Shale|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27724|Breakaway Shale|37568|5|Briefly described|p84|||||||||
27724|Breakaway Shale|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27724|Breakaway Shale|38232|6|Mentioned|p89|||||||||
27724|Breakaway Shale|38276|6|Mentioned|p166|||||||||
27724|Breakaway Shale|38348|6|Mentioned|p9|||||||||
27724|Breakaway Shale|38350|4|Described|p15|||||||||
27724|Breakaway Shale|38442|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of the Mount Isa Group.  Overlies the Moondarra Siltstone.||||||25-AUG-04
27724|Breakaway Shale|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27724|Breakaway Shale|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27724|Breakaway Shale|39445|5|Briefly described|Table 2|||||||||
27724|Breakaway Shale|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
27724|Breakaway Shale|39561|6|Mentioned|Fig.8|||||||||
27724|Breakaway Shale|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group. Grey siliceous siltstone and shale.||||||15-JUN-06
27724|Breakaway Shale|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27724|Breakaway Shale|40598|6|Mentioned|p28|||||||||
27724|Breakaway Shale|40623|5|Briefly described|p95|||||||||
27724|Breakaway Shale|41248|6|Mentioned|Fig.2|||||||||
27724|Breakaway Shale|41298|6|Mentioned|Map legend|Carpentarian||||||||
27724|Breakaway Shale|41307|4|Described|p16|||||||||
27724|Breakaway Shale|42350|6|Mentioned|Fig.1 P543|||||||||
27724|Breakaway Shale|42782|6|Mentioned|p458|||of Mount Isa Group||||||
27724|Breakaway Shale|44517|2|Defined|p234,235,map||Paleoproterozoic|Replaces "Hospital Shale". Unit of Mount Isa Group.||||||07-NOV-08
27724|Breakaway Shale|45072|6|Mentioned|p8|||Mount Isa Group||||||
27724|Breakaway Shale|45136|3|Fully described|p24|||||||||
27724|Breakaway Shale|45161|5|Briefly described|Table 8|||||||||
27724|Breakaway Shale|45166|5|Briefly described|p28|||||||||
27724|Breakaway Shale|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
27724|Breakaway Shale|47083|5|Briefly described|p19|||Equivalent to Gunpowder Creek Formation. Of Mount Isa Group. Maximum thickness 150 m.||||||
27724|Breakaway Shale|50332|5|Briefly described|p21, p95|Proterozoic|Proterozoic|Of the Mount Isa Group. Underlain conformably by Moondarra Siltstone. Geological Province: Western Fold Belt Province.||||||07-FEB-11
27724|Breakaway Shale|50550|6|Mentioned|p1141 Fig.4||Statherian|Of Mount Isa Group. Geological Province: Western Fold Belt.||||||19-DEC-07
27724|Breakaway Shale|50624|5|Briefly described|p237 Fig.4||Statherian|Parent: Mount Isa Group||||||
27724|Breakaway Shale|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Isa Group. Carbonaceous, pyritic shale and siltstone.||||||
27724|Breakaway Shale|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Overlain by Native Bee Siltstone, underlain by Moondarra Siltstone. Geological Province: Western Fold Belt.||||||
27724|Breakaway Shale|61736|5|Briefly described|p673|Paleoproterozoic|Paleoproterozoic|Age: 1663+/-3Ma for a tuff sample.||||||
27724|Breakaway Shale|61923|5|Briefly described|p29 Fig.2, p30|||Of the Mount Isa Group. Thin layer of finely laminated, dark grey-black, carbonaceous shale. Overlies Moondarra Siltstone; underlies Native Bee Siltstone. Geological Province: Mount Isa Inlier. See also p34 Fig.6||||||
27724|Breakaway Shale|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1663Ma. Geological Province: Isa Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
27724|Breakaway Shale|62084|4|Described|p936 Fig.5|||Isa Superbasin. Mount Isa.|1663+/-8 Ma U-Pb SHRIMP (after Page et al. 2000)|Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
27724|Breakaway Shale|62535|5|Briefly described|p672-674|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.|1663 +/- 3 Ma.|Mount Isa Group.||||
27724|Breakaway Shale|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
27724|Breakaway Shale|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Gun Spuersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
27724|Breakaway Shale|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Gun supersequence.||||||
27724|Breakaway Shale|63114|5|Briefly described|p1253 Fig.2. |||Isa Superbasin. Appears only as Breakaway.||Of the Gun supersequence||||16-MAR-18
27724|Breakaway Shale|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
27724|Breakaway Shale|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
27724|Breakaway Shale|63866|5|Briefly described|p58|Statherian|Statherian|Isa Superbasin.|1663 +/- 3 Ma (Page et al., 2000)|Gun Supersequence||||
27724|Breakaway Shale|64250|6|Mentioned|p11 fig 3, p19||||1663 +/- 3 Ma (deposition).|Mount Isa Group||||
27724|Breakaway Shale|65396|6|Mentioned|p82, p175, p188, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Leichhardt River Fault Trough. Detrital zircon sources listed.|1663 +/- 3 Ma (depositional age).|Mount Isa Group||Overlies Moondarra Siltstone; overlain by Native Bee Siltstone.||
27724|Breakaway Shale|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1663 +/- 8 Ma (Page et al. 2000).|||||24-APR-12
27724|Breakaway Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Isa Superbasin.|1663 +/- 3 Ma.|Mount Isa Group.|||Grey siliceous siltstone and shale|
27724|Breakaway Shale|68542|6|Mentioned|p6|||||||Overlies Moondarra Siltstone, overlain by Native Bee Siltstone||
27724|Breakaway Shale|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Moondarra Siltstone. Is overlain by Native Bee Siltstone.||
27724|Breakaway Shale|68732|6|Mentioned|p160, p162, p165 Fig.3, p168 Fig.5, p169|Statherian|Statherian|Of the Gun Supersequence. Sedimentary depositional age.|1655 +/- 4 Ma||||Characterised by monotonous intervals of massive- to finely laminated siltstone and shale, up to several hundreds of metres thick.|
27724|Breakaway Shale|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||Mount Isa Group||||
27724|Breakaway Shale|69591|5|Briefly described|p43 Fig.2.31, p45, p55|||Isa Superbasin. Part of Gun Supersequence. Deposited below storm base.||Mount Isa Group.|||Grey siliceous siltstone and shale.|
27724|Breakaway Shale|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Grey siliceous siltstone and shale.|
27724|Breakaway Shale|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Grey siliceous siltstone and shale.|
27724|Breakaway Shale|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1663+/-3 Ma (MDA: U-Pb zircon SHRIMP)||||Tuff in shale.|
27724|Breakaway Shale|71960|4|Described|p85-86, p77, p82, 83, 87, 101, 103|Proterozoic|Proterozoic|Thickness range 400 - 650 m. See description of 'Facies B' in Hero Syncline, p93-95.||Of Mount Isa Group.||Conformably overlies Moondarra Siltstone. Gradational with overlying Native Bee Siltstone.|Pale grey or orange and purple laminated silty shale; vuggy, sericitic, siliceous, and includes siltstone laminae 1-7mm thick. Massive shale in places and pyrite clasts.  In part fine-grained (pebbly) wacke facies in Hero Syncline.|
27724|Breakaway Shale|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|Paroo Range, Hero/Western Fault Zone.||Of Mount Isa Group|||Shale; fine grained pebbly wacke.|
27724|Breakaway Shale|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Age given as U-Pb zircon sedimentary depositional age.|1663 +/-3 Ma|Mount Isa Group||Overlies Moondarra Siltstone and underlies Native Bee Siltstone.||
27724|Breakaway Shale|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. U-Pb zircon sedimentary depositional age given.|1633 +/- 3 Ma|Mount Isa Group||Overlies Moondarra Siltstone and underlies Native Bee Siltstone.||
27724|Breakaway Shale|73042|6|Mentioned|p4|Statherian|Statherian|Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1663 +/- 3 Ma|Mt Isa Group||Underlain by Moondarra Siltstone. Overlain by Native Bee Siltstone.||
27724|Breakaway Shale|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Leichhardt River Domain.|1663+/-3 Ma crystallisation age of volcanic rock||||Carbonaceous shale (-silt) carbonates.|
81760|Breakfast Creek Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Eastern Fold Belt, Mount Isa area.|1758 +/- 8 Ma.|||||
27972|Breccia Creek Rhyolite|23423|5|Briefly described|p306 Table 7.3|Early Permian|Late Carboniferous|Timber Top Volcanic Subgroup of Featherbed Volcanic Group.||||||
27972|Breccia Creek Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
27972|Breccia Creek Rhyolite|43259|6|Mentioned|Appendix 1,p11.|Early Permian|Late Carboniferous|||||||
27972|Breccia Creek Rhyolite|43285|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Timber Top Volcanic Subgroup.||||||
27972|Breccia Creek Rhyolite|43567|5|Briefly described|Table 1,p400|||||||||
27972|Breccia Creek Rhyolite|43625|5|Briefly described|p36|||||||||
27972|Breccia Creek Rhyolite|43626|6|Mentioned|Table 1, p15|||||||||
27972|Breccia Creek Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgroup. Geological Province: Kennedy Province.||||||
27972|Breccia Creek Rhyolite|60425|5|Briefly described|p46 Tb. 3||Early Permian|Of Timber Top Volcanic Subgroup (Featherbed Volcanic Group). A-type rocks.||||||07-FEB-11
27972|Breccia Creek Rhyolite|62523|4|Described|p6-7, p3-4 (map/legend)|Early Permian|Late Carboniferous|Rhyolitic ignimbrite, crystal-poor to moderately crystal-rich; lithic clasts; lenticular vitriphyre, non-welded pyroclastics. Thick: ~250m. Unconformable on Hodgkinson Fm and uncomformable below Mt Mulligan Coal Measures.||||||07-FEB-11
30705|Briar Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30705|Briar Granite|50536|5|Briefly described|p1.4, 8.2 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30705|Briar Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite|||Leucocratic (biotite)-muscovite granite, porphyritic biotite granite.|
30705|Briar Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Leucocratic (biotite)-muscovite granite, porphyritic biotite granite.|
24766|Brighton beds|12597|5|Briefly described|p492 Tb.1, p494, p501|Toarcian|Pliensbachian|Nambour Basin. This name refers to the upper 200m of the Landsborough Sandstone. Contains thin coal seams of no apparent commercial value.||||||
24766|Brighton beds|42316|5|Briefly described|p8|||Variation on old name Brighton Beds?||||||
24766|Brighton beds|42893|6|Mentioned|p11|||||||||
24766|Brighton beds|60997|6|Mentioned|p140|||Part of Landsborough Sandstone in the Nambour Basin?||||||
24766|Brighton beds|60998|6|Mentioned|p144|Early Jurassic|Early Jurassic|Contains a ferruginous oolite marker bed. ||||||
24766|Brighton beds|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Early Jurassic|Southern Nambour Basin. Correlates with Evergreen Formation (Surat Basin) and Ma Ma Creek Member (Clarence-Moreton Basin). An alternative name for the upper 200 m of the Landsborough Sandstone.||Unit in Marburg Subgroup.||||
24766|Brighton beds|67402|5|Briefly described|p239, p254|Pliensbachian|Hettangian|Nambour Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a shoreline swamp environment with minor periodic marine incursions. 200m thick. |||||Thinly bedded sandstones, siltstone and shale with thin oolitic ironstone beds.|
24766|Brighton beds|68008|5|Briefly described|p238|Early Jurassic|Early Jurassic|Nambour Basin. Coeval with Evergreen Formation on the basis of a distinctive ooiltic ironstone marker bed.||||||
24766|Brighton beds|68135|5|Briefly described|p52 fig 2b|Toarcian||Southern Nambour Basin. Contains plant macrofossils. ||||Overlies Landsborough Sandstone.|Sandstone with oolitic ironstone beds.|14-SEP-17
24766|Brighton beds|69594|4|Described|p519, p545-547, p572|Early Jurassic|Early Jurassic|Jones and de Jersey (1947); Woods (1947). Southern Nambour Basin. Has been included as part of the Landsborough Sandstone (Cranfield et al., 1986 and others) or of the Marburg Formation (Cranfield et al., 1976).||Marburg Subgroup.||Overlies Landsborough Sandstone. Equivalent to Marburg Subgroup. Age-equivalent of Tiaro Coal Measures, Ma Ma Creek Member and Westgrove Ironstone Member.|Sandy, micaceous shale with thin red and white argillaceous and micaceous sandstone, minor coal laminae. Contains the distinctive Toarcian ferruginous oolite marker bed (Woods, 1947).|
23419|Brigooda Basalt|39970|3|Fully described|p61|||||||||
23419|Brigooda Basalt|40542|6|Mentioned|p98|||||||||
23419|Brigooda Basalt|43858|4|Described|32,33||Early Miocene|Age: 17.8+-0.2 Ma||||||
23419|Brigooda Basalt|61155|5|Briefly described|p20|Middle Miocene|Early Miocene|Age: 19-16.5Ma. In the Bundaberg-Maryborough region. ||||||
77687|Brinagee Schist|68350|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.||Unit in Argentine Metamorphics.||Is overlain conformably by Paynes Lagoon Amphibolite.|Fine-grained mica schist, quartzite and subordinate laminated amphibolite.|
77687|Brinagee Schist|68351|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.||Unit in Argentine Metamorphics.||Is overlain conformably by Paynes Lagoon Amphibolite.|Fine-grained mica schist, quartzite and subordinate laminated amphibolite.|
77687|Brinagee Schist|68419|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Of the Cape River Province.||Of the Argentine Metamorphics.||Conformably overlain by the Paynes Lagoon Amphibolite.|Fine-grained mica schist, quartzite and subordinate laminated amphibolite.|
77687|Brinagee Schist|68420|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Cape River Province. Minimum age shown as possibly Ordovician.||Of the Argentine Metamorphics.||Conformably overlain by the Paynes Lagoon Amphibolite.|Fine-grained mica schist, quartzite and subordinate laminated amphibolite.|
39711|Brisbane Valley Porphyrite|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Porphyritic hornblende diorite and microdiorite.||||||
39711|Brisbane Valley Porphyrite|68679|5|Briefly described|p427|Late Triassic|Late Triassic|Esk area. Previously assigned as Early-Middle Triassic.|223.6 Ma (K-Ar: Webb and McDougall, 1967).|||Intrudes the Esk Formation.|Porphyritic hornblende diorite and microdiorite.|
23421|Briscoe Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Shallow marine deposits.  Of the Gilbert River Formation.||||||
23421|Briscoe Member|42061|5|Briefly described|p153|||See also Fig.4||||||
38260|Brittania Basaltic Andesite|23764|4|Described|p346|||||||||
25812|Brittania Granodiorite|22847|3|Fully described|p 55|Early Devonian|Late Silurian|||||||
25812|Brittania Granodiorite|42633|5|Briefly described|Table 1 P9|||Reserved as Brittania Granite.||||||
25812|Brittania Granodiorite|42750|2|Defined|p44|Early Devonian|Late Silurian|||||||
25812|Brittania Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
25812|Brittania Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
34672|Brittania Supersuite|22847|5|Briefly described|p 13|||||||||
34672|Brittania Supersuite|23422|4|Described|p176, p213 Table 6.8|||Possibly late Silurian to early Devonian in age.  Made up of five plutons that intrude the Seventy Mile Range Group.||||||
34672|Brittania Supersuite|62521|5|Briefly described|p54-55|Devonian|Silurian|Comprises Black Jack and Policeman Creek Granodiorites, Flora Creek Trondhjemite and Brittania Granite. Geological Province: Ravenswood Batholith. Completely peraluminous, except for Policeman Creek Granodiorite.||||||14-JAN-08
34672|Brittania Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
34672|Brittania Supersuite|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.||||Intrudes Seventy Mile Range Group.|Medium-K to low-K, high-Na granites.|
78571|Brittany Suite|68731|5|Briefly described|p148|Ordovician|Ordovician|(Hutton et al. 1994a; Hutton and Rienks 1997). A tentative Ordovician age is assigned on the basis of strained quartz and recrystallised biotite. See also Brittany Supersuite.|||||Comprises pink to buff, fine- to coarse-grained, porphyritic hornblende-biotite granite.|
34664|Brittany Supersuite|22847|6|Mentioned|p 10|||||||||
34664|Brittany Supersuite|23422|4|Described|p173, p210 Table 6.6|||Probably Ordovician.||||||
34664|Brittany Supersuite|23430|5|Briefly described|p481 Fig 14.6|||Ravenswood Batholith Province.||||||
34664|Brittany Supersuite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
34664|Brittany Supersuite|23893|5|Briefly described|p12|Middle Ordovician|Late Cambrian|Geological Province: Macrossan Province.||||||
34664|Brittany Supersuite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Chipley, Columbia Creek (part), Hogsflesh and Lavery Creek Supersuites; Schreibers and Sunburst Suites; the Lynwater Complex; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
34664|Brittany Supersuite|68731|6|Mentioned|p149|||See also Brittany Suite.||||||
32129|Broadlands Granite|23037|5|Briefly described|p72,3|Permian|Carboniferous|||||||
32129|Broadlands Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgbl].  Pink, fine- to medium-grained biotite granite.||||||
32129|Broadlands Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink, fine- to medium-grained biotite granite; with possible zone of potassic alteration.||||||
32129|Broadlands Granite|65388|4|Described|p245-246, p236 Fig. 81, p237, 238,255|Early Permian|Late Carboniferous|Auburn Arch. Intrudes Boam Creek Quartz Monzodiorite and Torsdale Volcanics. Compared with Mount Appenben Granite, Glenleigh Granite. Pink, fine to medium-grained biotite granite. Poor outcrop over much of the unit. Age uncertain. ||||||
32129|Broadlands Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age uncertain.||||Intrudes Boam Creek Quartz Monzodiorite and Torsdale Volcanics.|Fine- to medium-grained biotite granite.|
41799|Broadsound Range Rhyolite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich, generally lithic poor, locally fiamme bearing, rhyolitic ignimbrite; aphyric to sparsely porphyritic rhyolite flows and high level intrusives.||||||
41799|Broadsound Range Rhyolite|60481|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich, generally lithic poor, locally fiamme bearing, rhyolitic ignimbrite; aphyric to sparsely porphyritic rhyolite flows and high level intrusives.||||||
41799|Broadsound Range Rhyolite|65388|5|Briefly described|p86, Fig. 35, p90 Fig. 37, p95, 353, 354|||Misspelling of Broadsound Range Volcanics? Age of southern sample within error of Bora Creek Quartz Monzodiorite age.||||||
41799|Broadsound Range Rhyolite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Ignimbrite.|
36273|Brodies Camp Supersuite|23291|4|Described|p46,p97 Tb. 3.11|Early Permian|Early Permian|Geological Province: Georgetown Region||||||
36273|Brodies Camp Supersuite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36273|Brodies Camp Supersuite|68405|5|Briefly described|Map Legend|Permian|Permian|Kennedy Province? Early Permian ? See map legend for lithological description.|||Includes Knob Camp Granodiorite. Includes two additional informal subdivisions.|Younger than Bulleringa Volcanic Subgroup.|Porphyritic biotite-hornblende granodiorite; fine- to coarse-grained porphyritic biotite granite.|
36273|Brodies Camp Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36273|Brodies Camp Supersuite|69593|4|Described|p484-485, p487, p489|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Occurs in the vicinity of Scardons Volcanic Group. Outcrop area ~30 km2. Early Permian?; one unit intrudes ~290 Ma volcanic rocks. Possibly co-magmatic with Permian units of Scardons Volcanic Group.|~290-280 Ma.||Knob Camp Granodiorite, Aylesbury Microgranite.||Hornblende-biotite and biotite-hornblende granodiorite, hornblende-biotite and biotite granite; rhyolite. A-type.|
28306|Broken River Group|23032|4|Described|p25,26,53 fig6|Middle Devonian|Early Devonian|||||||
28306|Broken River Group|23424|5|Briefly described|Table 8.1 Fig 8.3 p335.||Middle Devonian|Listed as Broken River Group (upper part). Of White (1965) and Wyatt & Jell (1980). Geological Province Graveyard Creek Subprovince.||||||
28306|Broken River Group|23430|4|Described|p479, p504-505|||Upper and Lower also see p479 and Plate 14.11. Overlying Unit Bundock Creek Group - unconformable. Underlying Unit Shield Creek Formation - unconformably. Graveyard Creek Subprovince.||||||20-MAY-15
28306|Broken River Group|23522|5|Briefly described|p259|Givetian|Late Silurian|||||||
28306|Broken River Group|24250|5|Briefly described|p121, 123|Devonian|Devonian|||||||
28306|Broken River Group|24577|5|Briefly described|p754 Fig. 2|Devonian|Devonian|Geological Province: Broken River Region, Lachlan Fold Belt.||||||
28306|Broken River Group|24610|6|Mentioned|p71|||||||||
28306|Broken River Group|24611|5|Briefly described|p194|Emsian|Emsian|Geological Province: Broken River Province.  See also p196 Fig. 2.||||||
28306|Broken River Group|24612|6|Mentioned|p13|||||||||
28306|Broken River Group|24613|5|Briefly described|p6 Fig. 3, p131|Middle Devonian|Early Devonian|Geological province: Burdekin Basin.||||||07-FEB-11
28306|Broken River Group|24614|5|Briefly described|p191 Fig. 1|||Includes the Mytton Formation.  Geological Province: Broken River Province.||||||07-FEB-11
28306|Broken River Group|41260|3|Fully described|p49|||See also p97 and p107. Briefly described Fig.18||||||20-MAY-15
28306|Broken River Group|41679|1|Redefined|p255|Frasnian|Emsian|Age: Emsian to early Frasnian.||||||
28306|Broken River Group|41719|6|Mentioned|p213|||See also Fig.2||||||
28306|Broken River Group|41739|6|Mentioned|p300|||||||||
28306|Broken River Group|41916|6|Mentioned|p28|||||||||
28306|Broken River Group|42031|4|Described|p760|||||||||
28306|Broken River Group|42032|5|Briefly described|p500|||||||||
28306|Broken River Group|42054|6|Mentioned|p273|||||||||
28306|Broken River Group|42279|6|Mentioned|Fig.2 P18|||||||||
28306|Broken River Group|42692|5|Briefly described|map legend|Devonian||||||||
28306|Broken River Group|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
28306|Broken River Group|42709|6|Mentioned|map legend|||||||||
28306|Broken River Group|42752|5|Briefly described|p47|||see also Fig.3 p47.||||||20-MAY-15
28306|Broken River Group|42933|1|Redefined|p79, Table 2|Middle Devonian||||||||
28306|Broken River Group|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
28306|Broken River Group|44516|14|Not recorded|p31|||Reference to geological map QLD 1953. See also Lexicon.||||||
28306|Broken River Group|44739|14|Not recorded|p19|||||||||
28306|Broken River Group|44740|14|Not recorded|p37,44,60,65|||||||||
28306|Broken River Group|44744|14|Not recorded|p106-109|||||||||
28306|Broken River Group|50077|5|Briefly described|p15|Early Devonian|Early Devonian|||||||
28306|Broken River Group|50093|4|Described|p237, p329 Fig.2|Givetian|Emsian|Limestone platform and submarine fan complex.||||||07-FEB-11
28306|Broken River Group|61727|5|Briefly described|p942 Fig.1|Devonian|Devonian|Geological Province: Broken River Province/Graveyard Creek Subprovince.||||||
28306|Broken River Group|63152|5|Briefly described|p120 Fig. 3|Devonian|Devonian|Includes Mytton and Papillio Formations, Dosey and Lomandra Limestones, Bracteata Formation and undifferentiated Broken River group units.||||||20-MAY-15
28306|Broken River Group|63154|5|Briefly described|p281 Fig. 3|Late Devonian|Early Devonian|Includes Wando Vale Subgroup. Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
28306|Broken River Group|64707|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Includes Wando Vale Subgroup. Mudstone, sandstone, conglomerate, limestone.||||||
28306|Broken River Group|65214|6|Mentioned|p272, p277|Devonian|Devonian|QLD NORTH and Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28306|Broken River Group|66498|6|Mentioned|p43, 47|Carboniferous|Emsian|Contains rich invertebrate micro- and macro-remains assemblages at all levels.||||||
28306|Broken River Group|67402|6|Mentioned|p244|||||||Disconformably overlain by the Bundock Creek Group.||
28306|Broken River Group|67848|5|Briefly described|p3 Fig.2.|Devonian|Devonian|Part of forearc basin component of the arc-trench gap succession involved in collisional accretion.||||||
28306|Broken River Group|68297|5|Briefly described|p193|Middle Devonian|Middle Devonian|See also Broken River Formation p183, p193. Includes Eifelian and Givetian limestones.||||||
28306|Broken River Group|68336|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Wando Vale Subgroup and Mytton Formation.|||
28306|Broken River Group|68338|5|Briefly described|Map legend.|||Graveyard Creek Subprovince.|||Includes Wando Vale Subgroup.|||
28306|Broken River Group|68341|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Wando Vale Subgroup and Mytton Formation.|||
28306|Broken River Group|68478|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Mytton Formation and Wando Vale Subgroup.|||
28306|Broken River Group|68479|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Mytton Formation and Wando Vale Subgroup.|||
28306|Broken River Group|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Broken River Province. This unit, as well as the Shield Creek Formation, Blue Rock Creek beds and Conjuboy Formation, are all mapped under the symbol, Db.||||||
28306|Broken River Group|69030|5|Briefly described|p6, p15, p17, p40|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province). Hosts significant gold mineralisation.|||Wando Vale Subgroup; Mytton Formation.||Marine shelf clastic rocks and limestone.|
28306|Broken River Group|69079|5|Briefly described|p5-6, p63, p67-68|Early Carboniferous|Devonian|Graveyard Creek Subprovince, Broken River Province. Hosts gold-antimony mineralisation in quartz veins, and sporadically-distributed antimony mineralisation in fissure veins (described in some detail).|||Mytton Formation, Papilio Mudstone, Dosey Limestone.||Contains intensely folded and faulted sedimentary rocks.|
28306|Broken River Group|69592|4|Described|p251 Fig.4.35, p258-259, p263-267, p272|Middle Devonian|Early Devonian|See also p274 Fig.4.65, p276-277, p296-298, p303. Originally the Broken River Formation of White (1965), for Devonian marine strata characterised by limestone. Wyatt and Jell (1980) separated the basal part of White's unit as the Shield Creek Formation, which is here assigned to the Graveyard Creek Group. Jell (1968) named several limestone intervals as Members. Raised to Group status by Withnall et al. (1988) and Lang et al. (1989, 1993) to comprise the Wandovale Subgroup and the overlying Mytton Formation. Graveyard Creek Subprovince, Broken River Province. Up to 1400m thick. Fence diagram. Deformation described.|||Bracteata Mudstone; Burges, Lomandra, Papillio, Mytton Formations; Dosey Limestone.|Overlies Graveyard Creek Group. Is overlain unconformably by Bundock Creek Group. Is faulted against Mytton Formation.||
28306|Broken River Group|73201|6|Mentioned|p609, p610|Devonian|Silurian|Broken River Province, Graveyard Creek Subprovince. Predominantly shallow marine strata. Setting interpreted as a forearc basin.||||||
35393|Bromley Hills Formation|61392|4|Described|p163-165, p170|Early Carboniferous|Middle Devonian|Of the Silverwood Group (Keinjan Terrane). Sand-rich point-source submarine fan. Max. thickness: 1720m.||||||07-FEB-11
35393|Bromley Hills Formation|63731|5|Briefly described|Map legend||Silurian|Of Silverwood Group. Includes the Long Mountain Breccia Member. Very thick-bedded, amalgamated, coarse, volcaniclastic arenite; and thin-bedded volcaniclastic arenite/mudstone turbidites punctuated by gravel-rich bands and debris-flow deposits.||||||12-DEC-07
35393|Bromley Hills Formation|63748|4|Described|p7 Fig. 3, p8|Late Devonian|Middle Devonian|Of Silverwood Gp. Includes Long Mountain Breccia Member at base. Unconformable on Bald Hill Fm and Ormoral Volcanics; unconformable below Eight Mile Creek beds. Max.thickness: ~1720m. Geol.Prov: Silverwood province. Sand-rich volcaniclastic turbidites.||||||07-FEB-11
35393|Bromley Hills Formation|68679|4|Described|p445-447|Mississippian|Middle Devonian|Van Noord (1999). Silverwood Province. ~1720m thick. Sandy volcaniclastic turbidites. Similar to parts of the Texas beds.||Topmost Silverwood Group.|Long Mountain Breccia Member.|Unconformably overlies Bald Hill Formation and Ormoral Volcanics. Is faulted locally against Bald Hill Formation and Connolly Volcanics. Is overlain by Eight Mile Creek beds.|Basal polymict megabreccia overlain by two units: one typified by thin-bedded turbidites with interbedded gravel-rich bands and debris-flow deposits, and a second unit dominated by very thick-bedded amalgamated coarse-grained turbidites.|
35393|Bromley Hills Formation|73600|6|Mentioned|p204|Devonian|Devonian|New England Orogen.||||||
23425|Bromley Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Shallow marine deposits.  Of the Garroway Sandstone.||||||
23425|Bromley Member|42061|5|Briefly described|Fig.4 P151|Late Jurassic|Middle Jurassic|Of Garraway Sandstone.  Olive River area, Carpentaria Basin.||||||
23425|Bromley Member|62837|5|Briefly described|Stratigraphic columns|Oxfordian|Bathonian|Of the Garraway Formation. Age: ~163-~151Ma. Geological Province: Northern Cape York.||||||01-MAR-10
24198|Bronco Stromatolith Bed|40686|2|Defined|p408|Ordian|Ordian|||||||
24198|Bronco Stromatolith Bed|40954|6|Mentioned|p133|||||||||
24198|Bronco Stromatolith Bed|41240|6|Mentioned|p112|||See also Fig.10||||||
24198|Bronco Stromatolith Bed|47058|6|Mentioned|Fig.4 P124|||||||||
24198|Bronco Stromatolith Bed|60122|6|Mentioned|p16|||Of Southgate (1986). A distinctive, thin 1-30cm marker bed of limonite-stained, stratiform to low-domical stromatolites.  May correlate with the former "Upper Hay River Formation Member 1" interval of the current Thorntonia Limestone.||||||
24198|Bronco Stromatolith Bed|64068|6|Mentioned|p57|||Northeastern Georgina Basin. Of Southgate (1986).||Of Thorntonia Limestone.|||Dolomitic-phosphatic.|05-APR-12
24198|Bronco Stromatolith Bed|65337|6|Mentioned|p60.|||Northeastern Georgina Basin. ||||||
24198|Bronco Stromatolith Bed|69443|5|Briefly described|p28:16-17|Middle Cambrian|Middle Cambrian|Southgate (1986), Shergold and Southgate (1986).||||Disconformably overlies Thorntonia Limestone.||12-JUL-16
24198|Bronco Stromatolith Bed|69591|6|Mentioned|p98 Fig.2.91|Middle Cambrian|Middle Cambrian|Appears in the body of the text as Bronco Stromatolith (see p88-89, p97). Occurs at the top of Thorntonia Limestone.||||||
24198|Bronco Stromatolith Bed|72516|6|Mentioned|p91|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Thorntonia Limestone.||02-JUN-21
30103|Brook Complex|22847|3|Fully described|p 8, 38|Early Devonian|Cambrian|||||||
30103|Brook Complex|23422|6|Mentioned|p209 Table 6.6|||||||||
30103|Brook Complex|23504|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
30103|Brook Complex|23513|5|Briefly described|Map legend|Ordovician||Palaeozoic Intrusive No. 490. I-Type.||||||
30103|Brook Complex|43093|4|Described|Appendex 1|||Probable Cambrian to Early Devonian. Metamorphic/granite complex.||||||
30103|Brook Complex|43259|4|Described|Appendix 1, p51.|Devonian|Cambrian|||||||16-APR-09
30103|Brook Complex|43936|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
75124|Brook granite|60425|4|Described|p98, p100, 288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name for felsic granite of Bedarra Suite (Bedarra Batholith or Supersuite) of Bedarra Granite Belt. Cut by dykes of more mafic North Island granite. Med.-gr., even-gr. to slightly porphyritic biotite granite; with biotite-rich schlieren. I-type.||||||07-FEB-11
29857|Brookdale Granite|22630|4|Described|p 50|Ordovician|Cambrian|||||||
29857|Brookdale Granite|22844|4|Described|Fig4  p50||Ordovician|Previously mapped in Ravenswood Granite Complex (Paine 1971)||||||
29857|Brookdale Granite|23049|3|Fully described|p62|Middle Devonian|Middle Devonian|||||||
29857|Brookdale Granite|23283|2|Defined|p27|Ordovician|Cambrian|||||||
29857|Brookdale Granite|23508|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
36225|Brookers Waterhole Granite|23291|5|Briefly described|p103, Tb.3.13|Late Carboniferous|Late Carboniferous|Intrudes Tate Batholith undivided; intruded by Soda Spring Granite and Branch Creek rhyolite (unassigned). Geological Province: Georgetown Region.||||||24-JUN-15
36225|Brookers Waterhole Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36225|Brookers Waterhole Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 367. I-Type.||||||
36225|Brookers Waterhole Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36225|Brookers Waterhole Granite|23624|4|Described|p14|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||24-JUN-15
36225|Brookers Waterhole Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, even-grained hornblende-biotite monzogranite.|
36225|Brookers Waterhole Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, even-grained hornblende-biotite monzogranite.|
29558|Broome Head Metamorphics|22740|4|Described|155,156 fig 2, 157|Paleozoic|Paleozoic|Geol province New England Fold Belt. Also on pages 158-160,162-166||||||07-NOV-08
29558|Broome Head Metamorphics|42980|5|Briefly described|Fig.4,p304|||||||||
29558|Broome Head Metamorphics|43754|4|Described|Fig.1p572, 574, 576|||Rb-Sr Age: 255 Ma. High grade equivalent of Shoalwater Formation, Townshend Formation.||||||01-MAR-10
29558|Broome Head Metamorphics|61035|5|Briefly described|p14|||Geological Province: Wandilla Province. Suite of metamorphic rocks, upper amphibolite facies. Four generations of folding is documented. Shear indicators suggest this unit has been thrust obliquely over the "Mount Holly Formation".||||||07-FEB-11
29558|Broome Head Metamorphics|65388|5|Briefly described|p153, p70 Fig. 28|||Wandilla Subprovince, northern Yarrol Province. Shoalwater Bay area. High grade equivalent of Curtis Island Group? Correlated with Marlborough Metamorphics||||||
29558|Broome Head Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Duckpond Road and Gaythorn Metamorphics, Sabina Point Schist, The Shacks Mylonite, Townshend Formation, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
29558|Broome Head Metamorphics|68679|5|Briefly described|p308-309, p312-313, p319, p347|Carboniferous|Late Devonian|Morand (1993); Leitch et al. (1994). Shoalwater Bay area, Wandilla Subprovince, Northern Yarrol Province. High-grade, multiply deformed. Seems to have the same protolith as Townshend Formation.||||Thrust over Erebus beds. Equivalent to Curtis Island Group.|Upper amphibolite grade; sillimanite-garnet gneiss, quartzite and amphibolite; commonly migmatitic and with four generations of folds.|
29558|Broome Head Metamorphics|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
29558|Broome Head Metamorphics|71702|6|Mentioned|p186, p187 Fig. 12|||||||||
34675|Broughton River Suite|22847|5|Briefly described|p 13|||||||||
34675|Broughton River Suite|23422|4|Described|p214 Table 6.8|||See also Broughton River Supersuite p176.||||||
34675|Broughton River Suite|62075|5|Briefly described|p10|||High-K calc-alkaline. Hosts some of the gold veins in the Charters Towers District. Appears as Broughton River suite.|||||Oxidised, I-type granitoids.|
34675|Broughton River Suite|62521|4|Described|p55, p59|Devonian|Silurian|Comprises Broughton River Granodiorite. Geological Province: Ravenswood Batholith. Zoned pluton ranging from two pyroxene-quartz monzodiorite at margin to granite at core.||||||21-DEC-07
34675|Broughton River Suite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
34675|Broughton River Suite|69592|5|Briefly described|p293-294|||Ravenswood Batholith, Charters Towers Province.|||Broughton River Granodiorite.|||
38177|Broughton River Supersuite|23422|4|Described|p176|Early Devonian|Early Devonian|See also Broughton River Suite p214 Table 6.8.||||||
33433|Brovinia beds|23799|6|Mentioned|p28|||Of Rockhampton Group.  Geological Province: Yarrol Province.||||||
36377|Brown Junction Formation|23425|5|Briefly described|p373 Fig 9.10|||Pascoe River Group Province.||||||
36214|Brown Mountain Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
36214|Brown Mountain Granite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36257|Brownville Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36257|Brownville Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36257|Brownville Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Included, in recent mapping, in Black Prince Granite together with Disaster, Glenlinedale, Stingo and Wilderness Granites. Fine-grained, porphyritic granite. I-type.||||||07-FEB-11
38038|Brumby Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Fine to medium grained, rarer coarse to granule sandstone; laminated, brecciated and stromatolitic chert; chert-clast breccia and conglomerate with sandstone matrix; siltstone and shale.||||||
38038|Brumby Formation|65337|3|Fully described|p9 Fig.5, p22 Table 4, pp24-26.|Paleoproterozoic|Paleoproterozoic|Southeast MOUNT DRUMMOND area. 350 - 800 m thick intertidal to supratidal including sabkha, deeper shelf in upper part, deposits. Forms low hills and plains adjacent to main ridges of Carrara Range.|1725 +/- 3 ma to 1658 - 1653 Ma.|Unit in McNamara Group.||Overlies Drummond Formation. Is overlain by Shady Bore Quartzite or Bullrush Conglomerate.|Interbedded fine- to medium-grained, rarer coarse to granule sandstone; laminated, brecciated and stromatolitic chert; chert-clast breccia and conglomerate with sandstone matrix; siltstone and shale dominate upper part.|
38038|Brumby Formation|69433|4|Described|p18:2, 6, 9|Statherian|Statherian|Rawlings et al. (2008); formerly part of the (now obsolete) Musselbrook Formation. Southern succession, Lawn Hill Platform. Absent from the Maloney Creek Inlier. 350-800m thick. Carbonate ramp deposits followed by deeper water (shelf) deposits.||McNamara Group.||Conformably overlies Drummond Formation. Is overlain conformably by Shady Bore Quartzite.|Siltstone, shale, sandstone and granule conglomerate, laminated and stromatolitic chert, dolostone, and chert-clast conglomerate and breccia. Finer lithologies become more abundant up-section.|
38038|Brumby Formation|69673|4|Described|p52 fig 42, p53|||Up to 800m thick. Deposited in carbonate ramp environment.||McNamara Group|||Siltstone, shale, sandstone and granule conglomerate, laminated and stromatolitic chert, dolostone and chert-clast conglomerate and breccia.|
38038|Brumby Formation|72526|5|Briefly described|p8 Fig.1.3, p10.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin. Unit located in the NT side of the McNamara Group.||McNamara Group||Overlies Drummond Formation and underlies Bullrush Conglomerate and Shady Bore Quartzite.||
38038|Brumby Formation|72527|4|Described|p1,p8, p91, p105-111, p112, p193, p194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Shift in provenance from underlying Drummond Formation. Considered to have been deposited in a mainly shallow marine environment with some deeper marine, low energy facies higher in the formation (Rawlings et al., 2008).|1671+/-12 Ma max dep age|McNamara Group||Conformably overlies Drummond Formation and underlies Shady Bore Quartzite. Considered to be laterally equivalent to Paradise Creek Formation.|Includes massively to thickly bedded, very fine-grained, very well-sorted and well-rounded quartz sandstone. Rounded quartz grains are mantled by interstitial quartz cement. Minor opaques are present (<1 percent).|
38038|Brumby Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Shown as being located in the Northern Territory part of the McNamara Group.||McNamara Group||Overlies Drummond Formation and underlies Shady Bore Quartzite and is partially equivalent to Fish River Formation and Bullrush Conglomerate.||
38038|Brumby Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Drummond Formation. Overlain by Shady Bore Quartzite.||
38038|Brumby Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Unconformably overlain(?) by Shady Bore Quartzite.||
38038|Brumby Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
36262|Brumby Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||07-OCT-08
36262|Brumby Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 285. I-Type.||||||
36262|Brumby Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36262|Brumby Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Medium- to coarse-grained, porphyritic biotite granite; I-type. Also includes Hayes Granite (informally referred to as Nantyeta granite) on most recent maps.||||||07-FEB-11
39025|Buaraba Granodiorite|23799|5|Briefly described|p12 Tb. 1, p94|Middle Triassic|Early Triassic|First mapped as Buaraba Quartz Diorite (Campbell 1952).  Granodiorite, leucogranodiorite, tonalite, quartz diorite. Age: 237+/-my (Rod Holcombe, pers. comm., 1999).  Intrudes South Buaraba Microdiorite.  Of SE Qld. Volcanic and Plutonic Intrusives||||||07-APR-08
39025|Buaraba Granodiorite|68679|5|Briefly described|p410, p414|||West of the Esk Basin, southern part of the northern New England Orogen.|237.9 +/- 7 Ma : Cranfield et al. (2001).|||Largely surrounds the South Buaraba Microdiorite.|Equigranular granodiorite to tonalite with some diorite along chilled margins.|
26428|Buaraba Mudstone|23799|3|Fully described|p34, p14 Tb. 1, p61 Fig. 4|Late Permian|Late Permian|Of Campbell (1952) and Allen (1972). Of Cressbrook Ck Gp. Overlies Box Gully Formation.  Geol.Prov: Cressbrook Creek Province. Mudstone sequence with minor interbedded arenite and conglom.  Intruded by "Champion Hills Diorite" and "Buaraba Granodiorite".||||||07-APR-08
26428|Buaraba Mudstone|23800|5|Briefly described|Map legend|Permian|Permian|Of the Cressbrook Creek Group.||||||
26428|Buaraba Mudstone|24560|5|Briefly described|Map legend|Permian|Permian|Of Cressbrook Creek Group.  Mudstone, arenite, conglomerate, andesite, basalt, tuffaceous sediments, locally bioturbated; rare marine fossils and plant fragments.||||||
26428|Buaraba Mudstone|29386|5|Briefly described|p454|||Permian.||||||
26428|Buaraba Mudstone|30471|6|Mentioned|p129|||||||||
26428|Buaraba Mudstone|31118|6|Mentioned|Table 1|||||||||
26428|Buaraba Mudstone|33381|4|Described|p109|||Permian. See also p111. Cressbrook Creek Group||||||07-APR-08
26428|Buaraba Mudstone|39252|6|Mentioned|Fig.13|||||||||
26428|Buaraba Mudstone|39445|5|Briefly described|Table 8|||||||||
26428|Buaraba Mudstone|42525|5|Briefly described|Map legend|Early Permian?|Early Permian?|Of the Cressbrook Creek Group.||||||15-JUL-04
26428|Buaraba Mudstone|42987|6|Mentioned|p30|||||||||
26428|Buaraba Mudstone|44555|4|Described|p223|||See also Lexicon.Unconformably overlain by Bundamba Sandstone.||||||
26428|Buaraba Mudstone|68679|5|Briefly described|p386|Guadalupian|Guadalupian|Cranfield et al. (2001). Cressbrook Basin. ~1200m thick. Shallow-marine, nearby terrestrial environment.||Cressbrook Creek Group.||Conformably overlies Box Gully Formation.|Mudstone (partly carbonaceous); thick massive or rhythmically interbedded with sandstone; minor conglomerate bands, local vesicular andesite and minor tuff locally. Has worm burrows, plant fragments, marine macrofossils.|
31110|Bubbling Granodiorite|23032|5|Briefly described|p39|||||||||
31110|Bubbling Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31110|Bubbling Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
31110|Bubbling Granodiorite|43480|2|Defined|7-19|Devonian|Silurian|||||||
31110|Bubbling Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
70410|Bucandy Creek Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Biotite granite; porphyritic biotite monzogranite.|
70410|Bucandy Creek Granite|68679|5|Briefly described|p421-422|Guadalupian|Guadalupian|Gayndah-Gladstone belt.|||||Porphyritic biotite monzogranite; weak to moderate foliation.|
25708|Buckabie Formation|22464|5|Briefly described|p9|Dinantian|Late Devonian|Adavale Basin. Overlies Etonvale Formation||||||
25708|Buckabie Formation|22518|5|Briefly described|p 10, Fig 3|||Adavale Basin||||||
25708|Buckabie Formation|22604|6|Mentioned|p442|||||||||
25708|Buckabie Formation|23522|5|Briefly described|p250 Fig 6|Late Devonian|Late Devonian|||||||
25708|Buckabie Formation|23834|4|Described|p314|Early Carboniferous|Late Devonian|Geological Province: Adavale Basin.  Maximum thickness:  2135m.||||||
25708|Buckabie Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
25708|Buckabie Formation|29387|6|Mentioned|Table 1|||Refers to Galloway(1970).||||||
25708|Buckabie Formation|29391|6|Mentioned|Table 2|||See P14.||||||
25708|Buckabie Formation|29393|6|Mentioned|Table 1|||Upper Devonian.||||||
25708|Buckabie Formation|29721|6|Mentioned|p38|||||||||
25708|Buckabie Formation|30103|4|Described|p5|||Table 2. U.Devonian - ?L.Carboniferous.See also Fig.1.||||||
25708|Buckabie Formation|30104|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25708|Buckabie Formation|30544|6|Mentioned|Fig.5 P51|||Devonian||||||
25708|Buckabie Formation|30691|6|Mentioned|p20|||||||||
25708|Buckabie Formation|30853|1|Redefined|p24|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25708|Buckabie Formation|30855|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25708|Buckabie Formation|31431|5|Briefly described|Table 2|||||||||
25708|Buckabie Formation|31436|6|Mentioned|Map legend|Early Carboniferous|Middle Devonian|Middle Devonian-Lower Carboniferous||||||
25708|Buckabie Formation|31438|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25708|Buckabie Formation|31999|5|Briefly described|p135|||See also Table 1||||||
25708|Buckabie Formation|32619|6|Mentioned|p463|||Late Dev.||||||
25708|Buckabie Formation|32865|4|Described|p483|||Late Dev. to early Carb.||||||
25708|Buckabie Formation|33069|4|Described|p6|||U.Dev. Adavale gp.||||||
25708|Buckabie Formation|33078|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25708|Buckabie Formation|33079|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25708|Buckabie Formation|33087|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Lower Carboniferous - Upper Devonian||||||
25708|Buckabie Formation|33088|4|Described|Table 2|||U.Dev.-L.Carb.||||||
25708|Buckabie Formation|33092|5|Briefly described|p5|||Stratigraphy||||||
25708|Buckabie Formation|33096|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
25708|Buckabie Formation|33192|6|Mentioned|p19|||||||||
25708|Buckabie Formation|33641|6|Mentioned|p58|||See also P59. U.Dev.||||||
25708|Buckabie Formation|34065|4|Described|p7|||U.Dev.-Carb?||||||
25708|Buckabie Formation|34217|6|Mentioned|Map legend|Carboniferous|Late Devonian|Upper Devonian - Carboniferous||||||
25708|Buckabie Formation|34218|5|Briefly described|Table 1|||Upper Devonian - Carboniferous. See also Table 2||||||
25708|Buckabie Formation|37565|6|Mentioned|Fig.6|||||||||
25708|Buckabie Formation|37610|6|Mentioned|Fig.4|||||||||
25708|Buckabie Formation|38226|5|Briefly described|p414|||||||||
25708|Buckabie Formation|39445|5|Briefly described|Table 6|||Correlated with Permo-Carb sediments of Cooper Basin. See also P82||||||
25708|Buckabie Formation|39478|6|Mentioned|Table 1|||||||||
25708|Buckabie Formation|39480|6|Mentioned|p188|||||||||
25708|Buckabie Formation|39482|6|Mentioned|Fig.5|||||||||
25708|Buckabie Formation|39494|6|Mentioned|Fig.3|||||||||
25708|Buckabie Formation|39847|6|Mentioned|p30|||||||||
25708|Buckabie Formation|40030|6|Mentioned|Fig.3|||||||||
25708|Buckabie Formation|40322|6|Mentioned|Fig.3|||||||||
25708|Buckabie Formation|40544|6|Mentioned|Fig.4|||||||||
25708|Buckabie Formation|41097|6|Mentioned|p163|||Mention Table 1||||||
25708|Buckabie Formation|41167|6|Mentioned|p397|||||||||
25708|Buckabie Formation|41198|6|Mentioned|p35|||See also Table 1||||||
25708|Buckabie Formation|41208|6|Mentioned|Fig.1|||||||||
25708|Buckabie Formation|41247|6|Mentioned|p126|||||||||
25708|Buckabie Formation|41289|6|Mentioned|p211|||||||||
25708|Buckabie Formation|41492|6|Mentioned|p160|||||||||
25708|Buckabie Formation|42042|6|Mentioned|p244|||||||||
25708|Buckabie Formation|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
25708|Buckabie Formation|42999|5|Briefly described|Table 1,p90||Late Devonian|||||||
25708|Buckabie Formation|43004|5|Briefly described|Table 1,p179|||||||||
25708|Buckabie Formation|43105|5|Briefly described|p11|||||||||
25708|Buckabie Formation|43461|14|Not recorded|p617,Table p618|||Approx. equivalent to Telemon Formation||||||
25708|Buckabie Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
25708|Buckabie Formation|43914|14|Not recorded|p1,3,5,9,14,25,Fig.3||Middle Devonian|||||||
25708|Buckabie Formation|43975|14|Not recorded|p1|||Devonian fossils.||||||
25708|Buckabie Formation|44091|14|Not recorded|p33,37|Carboniferous|Devonian|||||||
25708|Buckabie Formation|44419|14|Not recorded|p279|Carboniferous|Devonian|||||||
25708|Buckabie Formation|44770|14|Not recorded|p11,diag.p113,115||Late Devonian|Part of Adavale Group.||||||
25708|Buckabie Formation|44851|4|Described|p172|Carboniferous|Late Devonian|||||||
25708|Buckabie Formation|44852|14|Not recorded|p74|||Overlies Middle Devonian. Underlies Early Carboniferous.||||||
25708|Buckabie Formation|44855|14|Not recorded|p21|Early Carboniferous|Late Devonian|||||||
25708|Buckabie Formation|44889|4|Described|p160,164|Carboniferous|Devonian|||||||
25708|Buckabie Formation|44901|14|Not recorded|p3||Early Carboniferous|||||||
25708|Buckabie Formation|45073|6|Mentioned|p46|||U.Dev.-L.Carb. (?) P16.||||||
25708|Buckabie Formation|46881|6|Mentioned|Table 2|||||||||
25708|Buckabie Formation|48920|6|Mentioned|p13|||See also P85||||||
25708|Buckabie Formation|48951|6|Mentioned|p8|||||||||
25708|Buckabie Formation|48995|5|Briefly described|p3|||See also P59.||||||
25708|Buckabie Formation|62985|5|Briefly described|p16|Famennian|Frasnian|Uppermost formation in the Adavale Basin. Contains red beds of quartzose sandstone and mudstone of fluvial origin. Gas has been produced from the Gilmore gasfield.||||||02-JUL-14
25708|Buckabie Formation|64783|4|Described|p101-102, p82, 84, 96, 100,103, 104|Famennian|Frasnian|The name Buckabie beds was first used by Tanner (1962). Phillips Petroleum Company (1964) defined the type section of the unit between 1441.1m and 2683.46m in PPC Gumbardo-1. Galloway (1970) redefined the stratigraphic extent of the type section so that the lower limit is 2347m depth. Age is middle Frasnian to middle Famennian. Upper limit to Adavale Basin; unconformably overlain mainly by Galilee Basin strata.||||Overlies Etonvale Formation conformably, and Log Creek Formation unconformably.|Up to 1681.7m thick. Red-bed clastic succession that primarily consists of quartz sandstone, shale and conglomerate. Dolomitic, calcareous and red-clay cements are present.|15-NOV-17
25708|Buckabie Formation|65214|6|Mentioned|p282|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25708|Buckabie Formation|67402|4|Described|p167 fig ADV/WRR3, p168-p170|Famennian|Frasnian|Adavale Basin. Continental red bed deposits but partly deposited by a high energy fluvial system. See also p172, p173, p175.||||Overlies the Etonvale Formation.|Coarse-grained quartzose sandstone, shale and conglomerate.|
25708|Buckabie Formation|67561|6|Mentioned|p53 Fig.3|||||||||
25708|Buckabie Formation|68731|5|Briefly described|p177 Fig 3.91, p179, p180 Tb 3.3|Late Devonian|Late Devonian|Adavale Basin. ~ 118-1682 m thick. Cores display rip-up clasts, some conglomeratic rocks and cross-bedded sandstones, suggesting periods of high-energy fluvial deposition.||||Underlain by the Etonvale Formation.|Comprises a redbed clastic succession that primarily consists of quartz, sandstone, shale, and conglomerate. Dolomitic, calcareous and red-clay cements are present.|
25708|Buckabie Formation|73179|6|Mentioned|p1135 Fig.2, 1136|Famennian|Frasnian|Adavale Basin.||||Underlain by Etonvale Formation.|Fluvial red-beds|26-SEP-22
39028|Buckamara Igneous Complex|23799|6|Mentioned|p87 Tb. 10|||Informal name for sub-unit of Eskdale Igneous Complex.||||||
77826|Bucket Hole Metavolcanics|67323|5|Briefly described|p107; GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Post-Barramundi. Camooweal-Murphy Domain, Mount Isa Inlier. Informally divided into two unnamed units. Appears as Bucket Hole Formation in both Time-Space Plots.|1823 Ma.||||Felsic metavolcanics, schist, minor meta-arenite, quartzite, metasiltstone, amphibolite gneiss. Schistose amphibolite and amygdaloidal metabasalt; minor felsic metavolcanics, para-amphibolite|
77826|Bucket Hole Metavolcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, as well as Oroopo Metabasalt, Alpha Centauri Metamorphics and Kallala Quartzite, are all mapped under the symbol, -Pvo.||||||
77826|Bucket Hole Metavolcanics|69591|5|Briefly described|p29-30, p32, p58|Paleoproterozoic|Paleoproterozoic|Ardmore-May Downs Domain, Mount Isa Province. Appears as Bucket Hole Volcanics on p30.|1823 +/- 8 Ma (maximum depositional age).||||Felsic metavolcanics, schist, minor meta-arenite, quartzite, metasiltstone, schistose amphibolite and amygdaloidal metabasalt.|
77826|Bucket Hole Metavolcanics|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Statherian|Orosirian|Leichhardt River Domain.|<1823+/-8 Ma maximum depositional age||||Felsic extrusives, minor siliciclastics.|
27119|Bucklands Hill Diorite|22611|6|Mentioned|Fig2 P186||Cambrian|||||||
27119|Bucklands Hill Diorite|22847|5|Briefly described|p 36, Table 1|Middle Cambrian||Puddler Supersuite.||||||
27119|Bucklands Hill Diorite|23422|5|Briefly described|p170, 208|Middle Cambrian|Early Cambrian|Also p174. Dated 508 +/- 8Ma ie Early to Middle Cambrian.||||||07-DEC-04
27119|Bucklands Hill Diorite|23430|5|Briefly described|p461||Middle Cambrian|Intrudes Charters Towers Metamorphics. SHRIMP U-Pb zircon 508 +/- 7 Ma.||||||
27119|Bucklands Hill Diorite|23893|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|||||||
27119|Bucklands Hill Diorite|42633|6|Mentioned|p16|||Variation on Buckland Hill Diorite?||||||
27119|Bucklands Hill Diorite|42750|2|Defined|p33|Early Ordovician|Late Cambrian|||||||
27119|Bucklands Hill Diorite|43093|5|Briefly described|p11|||see also Fig.1.||||||
27119|Bucklands Hill Diorite|43103|5|Briefly described|p17, Fig.6.|||||||||
27119|Bucklands Hill Diorite|43259|4|Described|Appendix 1,p48.|Early Ordovician|Late Cambrian|||||||
27119|Bucklands Hill Diorite|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|Shown as part of the Seventy Mile Range Group, but this seems to be a drafting error, see 'Geology of the Ravenswood Batholith', 1997 (00/30577).||||||
27119|Bucklands Hill Diorite|50552|5|Briefly described|p1048 Fig.2||Cambrian|In Lolworth-Ravenswood Terrane.||||||24-NOV-04
27119|Bucklands Hill Diorite|62074|6|Mentioned|p1|||Paper (p1) says Charters Towers Metamorphics INCLUDES mafic bodies (Bucklands Hill Diorite).|c.507 Ma (Huttton and Rienks, 1997).|||||11-AUG-15
27119|Bucklands Hill Diorite|62075|6|Mentioned|p7, p9 Fig.2, p11 Fig.3|Middle Cambrian|Middle Cambrian|Appears throughout as Bucklands Hill diorite.||||Intrudes the Charters Towers Metamorphics.||
27119|Bucklands Hill Diorite|62521|5|Briefly described|p13|||Geological Province: Ravenswood Batholith. Comprises dark grey to black locally foliated medium- to fine-grained diorite in a series of elongate bodies with the Charters Towers Metamorphics - interpreted as mafic dykes. Mafic intrusive rocks.||||||14-JAN-08
27119|Bucklands Hill Diorite|68576|6|Mentioned|Q_11: p42|||Charters Towers.||||||
27119|Bucklands Hill Diorite|68731|5|Briefly described|p145, p151 Fig 3.51|Series 3|Series 2|(Hutton and Crouch 1993a, 1993b). Chemically shows MORB-type tholeiitic chemical trends.|508 +/- 7 Ma (Fanning 1995)|||Intrudes the Charters Towers Metamorphics.||
27119|Bucklands Hill Diorite|69952|5|Briefly described|p5, p94||||508 +/- 7 Ma (Hutton et al., 1997).|||Intrudes Charters Towers Metamorphics.||
27119|Bucklands Hill Diorite|70749|5|Briefly described|p43|Cambrian|Cambrian|Charters Towers Province. |508 +/- 7 Ma.|||||
27119|Bucklands Hill Diorite|71592|5|Briefly described|Appendix A.|||Macrossan Igneous Province, Thomson Orogen.|507+/-12 Ma (crystallisation: U-Pb zircon SHRIMP)||||Diorite.|
27119|Bucklands Hill Diorite|71966|5|Briefly described|p990|Late Cambrian|Late Cambrian|Geological province: Charters Towers Province, Thomson Orogen. |508+\-7 Ma|||||
40106|Bucknalla Gabbro|24615|5|Briefly described|CD||Triassic|[RJgbu].  Triassic - Jurassic? Layered olivine gabbro, gabbro, troctolite, ferrigabbro, anorthosite, plagioclase-bearing clinpyroxenite, microdiorite.||||||
40106|Bucknalla Gabbro|50317|5|Briefly described|Map Legend|Jurassic|Triassic|Layered olivine gabbro, gabbro, troctolite, ferrigabbro, anorthosite, plagioclase-bearing clinopyroxenite, microdiorite.||||||09-JUN-04
40106|Bucknalla Gabbro|65388|5|Briefly described|p323|Triassic|Permian|Northernmost of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton.||||||
40106|Bucknalla Gabbro|68008|2|Defined|p334, p346, p368, p436-438|Early Jurassic|Late Triassic|Originally referred to as the Westwood intrusion (Hansen, 1971) or the Westwood layered gabbro (Clifford, 1987). After the name Westwood Complex was used by Wood (1974) and Ford et al. (1976) for the W lobe of the Bouldercombe Igneous Complex, the name Bucknalla Complex was introduced by Carrigg et al. (1989) to avoid confusion. The name is here changed to Bucknalla Gabbro to reflect the dominant composition. Forms a triangular mass of sides c.3km long, immediately W of Westwood township. The name is derived from Bucknalla homestead. The type area (Carrigg et al., 1989) is the prominent ridge 2km SW of the Bucknalla homestead. Geophysics briefly described; part of Marlborough Gravity Ridge. Comprises 15 mappable, laterally discontinuous units; total thickness may be 2000m. Hosts minor Cu-Pd-Au-Pt mineralisation.|200.8 +/- 6 Ma (plagioclase: Holcombe et al.,1997)|||Intrudes Flaggy Quartz Monzodiorite and Rookwood Volcanics.|A layered gabbroic lopolith including gabbro, olivine gabbro, leucogabbro, anorthosite, hornblende gabbro, feldspathic clinopyroxenite, olivine clinopyroxenite and wehrlite; lesser troctolite and ferrigabbro.|
40106|Bucknalla Gabbro|68679|5|Briefly described|p423, p426|||Yarrol belt. A tilted saucer-shaped lopolith with 15 mappable but laterally discontinuous units each 1-50m thick. Hosts minor primary Cu-Pb-Au-Pt mineralisation.||||Intrudes Rookwood Volcanics and Flaggy Quartz Monzodiorite.|A layered gabbro suite (~2000m thick) of olivine gabbro, gabbro, troctolite, ferrogabbro and anorthosite with primary igneous layering, and an ultramafic suite of plagioclase-bearing clinopyroxenite that may underlie the "neck" of the intrusion.|
27076|Buffel Formation|13516|6|Mentioned|p145 fig 3|Early Permian|Early Permian|From Taroom Shelf, Bowen Basin. Age: APP31 - APP32.||||Overlies Camboon Volcanics.||
27076|Buffel Formation|22439|5|Briefly described|p15, Fig.2|Late Permian|Early Permian|Taroom Trough, Bowen Basin.||||||
27076|Buffel Formation|22973|5|Briefly described|p9 Fig.2|Early Permian|Early Permian|||||||
27076|Buffel Formation|22975|5|Briefly described|p34 Fig.6|Early Permian|Early Permian|||||||
27076|Buffel Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
27076|Buffel Formation|22980|5|Briefly described|p249 Fig.2|Early Permian|Early Permian|||||||
27076|Buffel Formation|23037|5|Briefly described|p40-3,48,59,60,1,4,5||Early Permian|Possible correlation with Narayen beds.||||||
27076|Buffel Formation|23042|4|Described|p42||Artinskian|||||||
27076|Buffel Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
27076|Buffel Formation|24491|5|Briefly described|p20|||Geological Province: Bowen Basin.||||||
27076|Buffel Formation|24552|5|Briefly described|p113|Artinskian|Artinskian|Geological Province: Bowen Basin, QLD. Contains bryozoans described herein.||||||07-FEB-11
27076|Buffel Formation|24615|5|Briefly described|CD|Permian|Permian|[Pbu].  Lithic sandstone, conglomerate, breccia, fossiliferous limestone, siltstone, mudstone.||||||
27076|Buffel Formation|29436|6|Mentioned|p319|||||||||
27076|Buffel Formation|29437|6|Mentioned|p150|||Permian||||||
27076|Buffel Formation|29964|6|Mentioned|p5|||||||||
27076|Buffel Formation|30141|5|Briefly described|p134|||||||||
27076|Buffel Formation|30449|6|Mentioned|p4|||Brachiopods||||||
27076|Buffel Formation|30450|6|Mentioned|Table 1|||Permian age||||||
27076|Buffel Formation|30451|4|Described|p50|||Refers Wass (1965)||||||
27076|Buffel Formation|30546|6|Mentioned|p107|||See also P109. Lower Permian age. Correlation||||||
27076|Buffel Formation|30743|6|Mentioned|p24|||On geological map||||||
27076|Buffel Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27076|Buffel Formation|31079|6|Mentioned|Fig. 6|||||||||
27076|Buffel Formation|31659|6|Mentioned|p106|||||||||
27076|Buffel Formation|32943|6|Mentioned|p106|||See also Fig.2.||||||
27076|Buffel Formation|32944|6|Mentioned|Fig.3|||Permian||||||
27076|Buffel Formation|32945|6|Mentioned|p88|||Permian||||||
27076|Buffel Formation|33774|3|Fully described|p34|||||||||
27076|Buffel Formation|34132|6|Mentioned|p2|||Lower Permian||||||
27076|Buffel Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
27076|Buffel Formation|34348|6|Mentioned|p20|||Lower Permian.||||||
27076|Buffel Formation|35145|6|Mentioned|p83|||||||||
27076|Buffel Formation|35284|6|Mentioned|Fig.1|||||||||
27076|Buffel Formation|35426|3|Fully described|p653|||||||||
27076|Buffel Formation|35845|6|Mentioned|p65|||||||||
27076|Buffel Formation|35862|6|Mentioned|p271|||||||||
27076|Buffel Formation|35873|6|Mentioned|Fig.38|||||||||
27076|Buffel Formation|36045|6|Mentioned|p333|||||||||
27076|Buffel Formation|36333|6|Mentioned|Map legend|Early Permian|Early Permian|Of the Back Creek Group.||||||15-JUL-04
27076|Buffel Formation|36739|6|Mentioned|Fig.2|||||||||
27076|Buffel Formation|36925|1|Redefined|p179|Early Permian|Early Permian|||||||
27076|Buffel Formation|37070|6|Mentioned|p69|||||||||
27076|Buffel Formation|37075|5|Briefly described|Table 1|||||||||
27076|Buffel Formation|37858|6|Mentioned|Fig.1|||||||||
27076|Buffel Formation|38204|4|Described|p72|||||||||
27076|Buffel Formation|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27076|Buffel Formation|39212|5|Briefly described|p12|||||||||
27076|Buffel Formation|39252|5|Briefly described|p20|||||||||
27076|Buffel Formation|39261|6|Mentioned|Fig.6|||||||||
27076|Buffel Formation|39263|6|Mentioned|p148|||||||||
27076|Buffel Formation|39273|6|Mentioned|p305|||||||||
27076|Buffel Formation|39307|6|Mentioned|p438|||||||||
27076|Buffel Formation|39445|5|Briefly described|Table 8|||||||||
27076|Buffel Formation|40091|6|Mentioned|p70|||||||||
27076|Buffel Formation|40093|6|Mentioned|p27|||||||||
27076|Buffel Formation|40094|6|Mentioned|p23|||||||||
27076|Buffel Formation|40539|6|Mentioned|Fig.2|||||||||
27076|Buffel Formation|41246|6|Mentioned|Map legend|Permian||||||||
27076|Buffel Formation|41546|4|Described|p157|||||||||
27076|Buffel Formation|41666|6|Mentioned|p1|||||||||
27076|Buffel Formation|42249|6|Mentioned|p21|||||||||
27076|Buffel Formation|42250|6|Mentioned|Fig.4 P31|||||||||
27076|Buffel Formation|42865|5|Briefly described|p18|||||||||
27076|Buffel Formation|43000|5|Briefly described|p107|||||||||
27076|Buffel Formation|43017|5|Briefly described|Fig.3,p375|||||||||
27076|Buffel Formation|43018|6|Mentioned|p392|||||||||
27076|Buffel Formation|43050|5|Briefly described|p4|||||||||
27076|Buffel Formation|43185|6|Mentioned|6,9||Early Permian|||||||
27076|Buffel Formation|43474|14|Not recorded|p60|||Permian fossils||||||
27076|Buffel Formation|43483|6|Mentioned|14||Permian|||||||
27076|Buffel Formation|43714|6|Mentioned|Fig.3,p5||Early Permian|||||||
27076|Buffel Formation|43994|14|Not recorded|Map Legend|||||||||
27076|Buffel Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
27076|Buffel Formation|44379|14|Not recorded|p19|||||||||
27076|Buffel Formation|44424|14|Not recorded|p293-301|||Represents lower part of Tiverton Subgroup.||||||
27076|Buffel Formation|44427|2|Defined|p159-161,164,165|Artinskian|Sakmarian|Mundubbera area.||||||
27076|Buffel Formation|44640|14|Not recorded|p30|||||||||
27076|Buffel Formation|44809|14|Not recorded|p279||Permian|Fauna.||||||
27076|Buffel Formation|44857|14|Not recorded|p96-98||Permian|||||||
27076|Buffel Formation|44858|14|Not recorded|p94||Artinskian|||||||
27076|Buffel Formation|44859|14|Not recorded|p68-71||Permian|Gastropods. Peruvispira parva, sp.nov.||||||
27076|Buffel Formation|45031|14|Not recorded|p7,11,19,27,88,100,||Permian|p106,108,112,116,Fig.3,Pl.1,4,5,7,9||||||
27076|Buffel Formation|45071|3|Fully described|Table 1|||||||||
27076|Buffel Formation|48898|5|Briefly described|p15|||L.Permian. See also PP25,32||||||
27076|Buffel Formation|48900|6|Mentioned|Table|||Opposite P84.||||||
27076|Buffel Formation|48919|4|Described|p20|||See also P21 L.Permian||||||
27076|Buffel Formation|48926|6|Mentioned|p42|||P42 et seq.||||||
27076|Buffel Formation|50214|5|Briefly described|Map Legend|Permian|Permian|Of Back Creek Group||||||17-MAY-04
27076|Buffel Formation|50215|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Back Creek Group. Lithic sandstone, conglomerate, breccia, fossiliferous limestone, siltstone. mudstone.||||||18-JUN-09
27076|Buffel Formation|50273|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Back Creek Group.  Lithic sandstone, conglomerate, breccia, fossiliferous limestone, siltstone and mudstone.||||||18-MAY-04
27076|Buffel Formation|50301|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Back Creek Group.||||||
27076|Buffel Formation|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Geological province: eastern margin Bowen Basin.||||||29-MAR-10
27076|Buffel Formation|60282|5|Briefly described|p7|Early Permian|Early Permian|Limestone and siliciclastic rocks.  Disconformably separated from the overlying lithologically similar Oxtrack Formation of Late Permian age.  Geological Province: Bowen Basin.||||||12-JUL-13
27076|Buffel Formation|60568|5|Briefly described|p381|Sakmarian|Sakmarian|Contains new bryozoan species described herein. Geological Province: Bowen Basin.||||||
27076|Buffel Formation|61076|5|Briefly described|p188 Fig. 2|Permian|Early Permian|Geological Province: Bowen Basin, Taroom Trough.||||||
27076|Buffel Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||17-MAR-09
27076|Buffel Formation|61772|6|Mentioned|p128 Fig. 2||Early Permian|Geological Province: Bowen Basin.||||||24-SEP-08
27076|Buffel Formation|61778|5|Briefly described|p238, p241||Early Permian|Geological Province: Bowen Basin.||||||07-FEB-11
27076|Buffel Formation|62357|6|Mentioned|p524 Fig. 7, p528|Middle Permian|Early Permian|Geological Province: Bowen Basin (Taroom Trough).||||||
27076|Buffel Formation|64429|5|Briefly described|p19, p20|Early Permian|Early Permian|Geological province: Bowen Basin. ||||||
27076|Buffel Formation|64856|4|Described|p42 Fig.2, p48-52|Artinskian|Artinskian|Wass (1965); redefined by Flood et al. (1981). Bowen Basin. Fossiliferous limestone, siltstone; minor sandstone. Overlies Camboon Volcanics, probably unconformably. Age from palynoflora (unit APP32). Max thickness in study area 100m. Correlated with Cattle Creek Formation, Aldebaran Sandstone in part.| | ||||28-NOV-17
27076|Buffel Formation|64857|5|Briefly described|p114, p113 Fig.3|||Bowen Basin. Mainly limestone, siltstone and lesser sandstone, mostly marine, overlying Camboon Volcanics. ||||||
27076|Buffel Formation|64858|5|Briefly described|p181, p180 Fig.2, p191|Early Permian|Early Permian|Includes coals.||||||30-NOV-09
27076|Buffel Formation|64859|5|Briefly described|p196, 225|Permian|Permian|Marine mudstones, sandstones, limestones. Gas source rocks.||||||
27076|Buffel Formation|65112|6|Mentioned|p316; Fig 4 p314|Early Permian|Early Permian|Post-extension stratigraphic sequences of the Taroom Trough. Overlies Camboon Volcanics.||||||15-JAN-15
27076|Buffel Formation|65113|5|Briefly described|p338, p345, Fig 4 p 340|Early Permian|Early Permian|Equivalent to the top of Early Permian volcanic pile in the Taroom Trough. Overlies the Camboon Volcanics.||||||29-MAR-10
27076|Buffel Formation|65114|5|Briefly described|p385 Fig.3, p394|Early Permian||Post-rift sedimentary rocks; overlie Camboon Volcanics||||||
27076|Buffel Formation|65115|5|Briefly described|p411, 413, Fig 2 p403|Early Permian|Early Permian|Overlying the Camboon Volcanics. Contains limestone, mudstone and siltstone. Part of Supersequence B.||||||
27076|Buffel Formation|65116|5|Briefly described|Fig 2 p436|Early Permian|Early Permian|Overlies the Camboon Volcanics in the Taroom Trough, Bowen Basin.||||||
27076|Buffel Formation|65118|6|Mentioned|p480, 491, Fig 2 p479|Permian|Permian|Overlies the Camboon Volcanics in the Taroom Trough, Bowen Basin.||||||
27076|Buffel Formation|65119|6|Mentioned|Fig 4 p510, Fig 5 p511|||Present in the Cockatoo Creek Well.||||||
27076|Buffel Formation|65388|3|Fully described|p159-165; p26, 27, 28, 31, 32, 43, 149|Kungurian|Asselian|Of Back Creek Group, Bowen Basin. Rocks originally included in Oxtrack Formation (1959). Defined by Wass (1965). Includes fossiliferous limestones originally reported as part of Camboon Volcanics. Overlies Camboon Volcanics conformably in places. Overlain by Oxtrack Formation conformably to disconformably?, Barfield Formation. Time equivalent to Collaroy Volcanics, Tiverton Formation, Yarrol Formation. Predominantly fossiliferous limestone, siltstone and minor sandstone in outcrop. More sandstone in subsurface. Represents major marine transgression. See also p166, 178, 186||||||
27076|Buffel Formation|66615|6|Mentioned|p2 Fig.1, p9|||Southern Taroom Trough, Bowen Basin.||||||
27076|Buffel Formation|67402|6|Mentioned|p21|Kungurian|Artinskian|Bowen Basin. ||||Overlies the Camboon Volcanics. Unconformably overlain by the Oxtrack Formation.||
27076|Buffel Formation|67669|5|Briefly described|p11|Early Permian|Early Permian|Of Bowen Basin.||||Overlain by Oxtrack Formation. Underlain by Camboon volcanics.||
27076|Buffel Formation|68008|5|Briefly described|p139, p162, p166, p569|Permian|Permian|Bowen Basin. Early Permian.||||May be partial time equivalent of Owl Gully Volcanics.||
27076|Buffel Formation|68679|5|Briefly described|p344,p353,p355,p360,p375,p378,p380-381|Artinskian|Artinskian|Waterhouse et al. (1981). Taroom Trough, Bowen Basin. Early Permian marine shelf deposits. 100m thick.||||Unconformably overlies Camboon Volcanics. Is overlain unconformably by Oxtrack Formation. Correlated with Narayen beds. Time-equivalent of Collaroy Volcanics.|Fossiliferous limestone, calcareous siltstone, volcaniclastic sandstone, breccia and conglomerate.|
76888|Bularnu Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin|||||Pebble to cobble conglomerate and medium to very coars sandstone near the base.  Most of this unit is very fine to fine sandstone and siltstone|
76888|Bularnu Formation|68146|4|Described|p3, p6, p83-90, p199, p211|||May Downs area, W of Mount Isa. Originally mapped as [part of] Torpedo Creek Formation; they share a similar age (Neumann et al., 2009). This MDA is c.40-50 m.y. older that the true stratigraphic age, based on underlying Surprise Creek Formation's age (c.1688 Ma). Whole-rock Sm-Nd isotopic data tabulated.|1738 +/- 9 Ma maximum depositional age.|||Overlies Surprise Creek Formation and (probably disconformably) the Saint-Smith Sandstone.|Medium- to thick-bedded and crossbedded, medium- to very coarse-grained quartzose sandstone with scattered pebbles of sandstone or quartzite and white quartz; basal conglomerate.|
76888|Bularnu Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Saint-Smith and Pilpah Formations under the symbol, -Pp.||||||
76888|Bularnu Formation|68575|4|Described|p37, p40|||Saint-Smith Range area, Mount Isa Region. A thick package of pebble to cobble conglomerate mapped (Mount Isa 1:250 000 sheet) as Torpedo Creek Quartzite; renamed as Bularnu Formation. Provenance (detrital zircon populations) is similar to Saint-Smith Formation but significantly different from Torpedo Creek Quartzite.|1738 +/- 9 Ma (Carson et al., 2011).|||Overlies Saint-Smith Formation unconformably or disconformably. Possible equivalent to upper part of Fiery Creek Volcanics.|A thick package of pebble to boulder conglomerate.|
76888|Bularnu Formation|69591|5|Briefly described|p29, p56|Paleoproterozoic|Paleoproterozoic|Mount Oxide Domain, Mount Isa Province. Part of the ?Prize Supersequence. Fluvial/shallow-marine deposits.|1738 +/- 9 Ma (Carson et al., 2011).||||Mostly very fine to fine sandstone and siltstone; pebble to cobble conglomerate and medium to very coarse sandstone near the base.|
76888|Bularnu Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1738+/-9 Ma (MDA: U-Pb zircon SHRIMP)||||Sedimentary.|
76888|Bularnu Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
79277|Bulburin Granite|67874|5|Briefly described|p1-2, p21, p24|Late Triassic|Late Triassic|These rocks were formerly part of Castletower Granite. Age is based on field relations (Purdy, 2010).||||Intrudes Bobby Volcanics.||06-NOV-15
79277|Bulburin Granite|68679|5|Briefly described|p422, p428, p431-432|Late Triassic|Late Triassic|Northern New England Orogen. Mapped as one unit with Molangul Granite on p428.|||||Pale pink, fine- to medium-grained, equigranular biotite granite; miarolitic. Includes a dioritic phase that forms small, pod-like bodies and has spectacular net-vein relationships with felsic phases.|
79277|Bulburin Granite|73450|6|Mentioned|p21|||Interpreted to pre-date Molangul Granite.||||||
23435|Bulgeri Formation|23032|4|Described|p30|Carboniferous|Late Devonian|||||||
23435|Bulgeri Formation|23291|4|Described|p81 Tb. 3.6|Frasnian|Frasnian|Parent: Bundock Creek Group. Thickness: ~1000m. Geological Province: Georgetown Region.||||||08-JUL-15
23435|Bulgeri Formation|23424|4|Described|Table 8.1 p336.|Famennian|Frasnian|Age: Late Devonian (Frasnian to Famennian); brachiopods. Lowermost unit of Bundock Creek Group. Of Bundock Creek Group, Bundock Basin. Underlying Unit Broken River Group (d). Maximum thickness 3660 m.||||||
23435|Bulgeri Formation|23430|4|Described|p506||Devonian|Also see Plate 14.11. Of Bundock Creek Group. Underlying Unit Broken River Group - disconformable. Bundock Basin Province. Maximum thickness 3660 m (in type section).||||||
23435|Bulgeri Formation|23431|5|Briefly described|p541|||||||||
23435|Bulgeri Formation|23619|5|Briefly described|p33 Table 1||Late Devonian|Bundock Basin Province.||||||
23435|Bulgeri Formation|24577|4|Described|p752 Fig. 1, p 754 Fig. 2|Famennian|Frasnian|Of the Bundock Creek Group. Overlain by the Turrets Formation. Disconformably / unconformably overlies the Mytton Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||17-JUN-13
23435|Bulgeri Formation|24613|6|Mentioned|p54|||Contains the Jamieson Member. Geological province: Bundock Basin.||||||07-FEB-11
23435|Bulgeri Formation|24614|5|Briefly described|p191 Fig. 1|||Of the Bundock Creek Group. Unconformable on Mytton Formation. Geological Province: Broken River Province.||||||07-FEB-11
23435|Bulgeri Formation|40675|6|Mentioned|Table 4A|||||||||
23435|Bulgeri Formation|40954|6|Mentioned|p132|||||||||
23435|Bulgeri Formation|41260|3|Fully described|p77|||||||||
23435|Bulgeri Formation|41679|6|Mentioned|p71|||||||||
23435|Bulgeri Formation|41719|6|Mentioned|Fig.2|||||||||
23435|Bulgeri Formation|41739|2|Defined|p301|Famennian|Frasnian|||||||
23435|Bulgeri Formation|42054|6|Mentioned|p273|||||||||
23435|Bulgeri Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
23435|Bulgeri Formation|42709|6|Mentioned|map legend|||||||||
23435|Bulgeri Formation|42933|3|Fully described|p129|||Of Bundock Creek Group.||||||04-FEB-08
23435|Bulgeri Formation|43113|5|Briefly described|Table 1,p20.|||||||||
23435|Bulgeri Formation|43213|6|Mentioned|p75|||Broken River Province. Contains marine sediments, recording the Westwood transgression of the triangularis-crepida Zones [Famennian].||||||
23435|Bulgeri Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bundock Creek Group.||||||
23435|Bulgeri Formation|43480|6|Mentioned|26||Late Devonian|||||||
23435|Bulgeri Formation|43603|5|Briefly described|p9|||||||||
23435|Bulgeri Formation|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Bundock Creek Group.||||||
23435|Bulgeri Formation|63154|5|Briefly described|p285 Fig. 5|Late Devonian|Late Devonian|Geological province: Georgetown Inlier. Sedimentary rocks.||||||11-APR-07
23435|Bulgeri Formation|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group. Lithofeldspathic to feldspathic sandstone, polymictic conglomerate + mudstone; local fine-gr. redbeds, red lithic sandstone + conglomerate and minor calcirudite (reworked from Waldo Vale Subgroup); local green to pink reworked tuff||||||
23435|Bulgeri Formation|65214|6|Mentioned|p280|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23435|Bulgeri Formation|66589|6|Mentioned|p180|Famennian|Frasnian|Case studies cited; not visited in the field by the authors of this study.||||||
23435|Bulgeri Formation|67402|4|Described|p239, p245 |Famennian|Frasnian|Bundock Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a distal to proximal alluvial plain to maringal marine and coastal plain environment. Maximum thickness of 3660m. ||||Overlain by the Turrets Formation.|Lithofeldspathic to feldspathic sandstone, conglomerate, mudstone, redbeds with minor calcirudite and tuff.|
23435|Bulgeri Formation|67788|6|Mentioned|p22|Late Devonian|Late Devonian|Mentioned in a list of units containing braided and low-sinuosity river deposits.|||Rockfields Member.|||
23435|Bulgeri Formation|68336|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince. Three named, and two un-named, sub-units are mapped separately.||Unit in Bundock Creek Group.|Includes Rockfields, Stopem Blockem Conglomerate, and Jamieson Members.||Lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone and conglomerate and minor calcirudite (reworked from the Wando Vale Subgroup); local green to pink reworked tuff.|23-MAR-15
23435|Bulgeri Formation|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone and conglomerate and minor calcilutite (reworked from the Wando Vale Subgroup); local green to pink reworked tuff.|
23435|Bulgeri Formation|68341|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince. Three named, and two un-named, sub-units are mapped separately.||Unit in Bundock Creek Group.|Includes Rockfields, Stopem Blockem Conglomerate, and Jamieson Members.||Lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone and conglomerate and minor calcirudite (reworked from the Wando Vale Subgroup); local green to pink reworked tuff.|23-MAR-15
23435|Bulgeri Formation|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Turrets Formation.|Lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone and conglomerate.|
23435|Bulgeri Formation|68478|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.|Includes Jamieson Member, Stopem Blockem Conglomerate Member, and Rockfields Member.|Conformably overlain by the Turrets Formation.|Undivided: lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone, conglomerate and minor calcirudite (reworked from Wando Vale Subgroup); local green to pink reworked tuff.|
23435|Bulgeri Formation|68479|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin. Includes 1 unnamed, separately mapped unit of red, coarse-grained lithic sandstone and conglomerate; minor fine-grained redbeds and calcirudite.||Of the Bundock Creek Group.|Includes Jamieson Member, Stopem Blockem Conglomerate Member, and Rockfields Member.|Conformably overlain by the Turrets Formation.|Undivided: Lithofeldspathic to feldspathic sandstone, polymictic conglomerate and mudstone; local fine-grained redbeds, red lithic sandstone, conglomerate and minor calcirudite (reworked Wando Vale Subgroup); local green to pink reworked tuff.|
23435|Bulgeri Formation|68731|6|Mentioned|p187|||Graveyard Creek Subprovince.||||||
23435|Bulgeri Formation|69030|5|Briefly described|p6|Devonian|Devonian|Bundock Basin (Broken River Province).||Bundock Creek Group.|Stopem Blockem Conglomerate Member.|||
23435|Bulgeri Formation|69592|3|Fully described|p259, p272-274, p276, p298-299|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. Highly variable thickness: 3.6km in the SE wedging out into Chinaman Creek Limestone in the NE; suggesting the Basin floor had significant relief. Contains a sporadic, fairly varied fossil suite. Depositional environments and provenance discussed: mainly sand-dominated alluvial plain systems.||Basal Bundock Creek Group.|Rockfields, Stopem Blockem Conglomerate, Jamieson, Members.|Unconformably overlies Mytton Formation or Chinaman Creek Limestone (Broken River Group). Is overlain conformably by Turrets Formation.|Quartzose to feldspathic sandstone with subordinate mudstone, conglomerate and siltstone; sporadic red mudstone beds are characteristic and commonly contain small calcareous nodules of pedogenic origin.|
23435|Bulgeri Formation|70740|5|Briefly described|p49|||Bundock Basin. ||||Potentially equivalent to the Mount Wyatt Formation.||
25817|Bulimba Formation|9528|5|Briefly described|Map legend|Tertiary|Late Cretaceous|Poorly sorted clayey quartz sandstone, commonly pebbly; pebbly clay-rich siltstone; mudstone; conglomerate; stream sediments in depressions.||||||24-JUN-04
25817|Bulimba Formation|9531|5|Briefly described|Map Legend|Tertiary|Late Cretaceous|Sandstone, siltstone, mudstone, conglomerate.||||||02-JUL-04
25817|Bulimba Formation|22780|5|Briefly described|map|Tertiary|Late Cretaceous|||||||
25817|Bulimba Formation|22781|4|Described|p44|Tertiary|Late Cretaceous|Karumba Basin||||||
25817|Bulimba Formation|23291|4|Described|p80 Tb. 3.6|Tertiary|Tertiary|Age: Early to Mid-Tertiary. Thickness: <10m. Geological Province: Georgetown Region.||||||25-JUN-15
25817|Bulimba Formation|23423|6|Mentioned|p267|||||||||
25817|Bulimba Formation|23425|4|Described|p393 Table 9.7.|||Also see p383. Karumba Basin Province.||||||25-JUN-15
25817|Bulimba Formation|23426|6|Mentioned|p403|||Probably equivalent to Fairview Gravel. Karumba Basin Province.||||||
25817|Bulimba Formation|23430|5|Briefly described|p526|||Unit is undated. Lithostratigraphic equivalent of Darai Limestone in Papua New Guinea. Karumba Basin Province. Maximum thickness 220 m.||||||
25817|Bulimba Formation|23496|5|Briefly described|Table 4, p60||Tertiary|~120m thick.||||||
25817|Bulimba Formation|23500|5|Briefly described|Map legend|Tertiary|Tertiary|Carpentaria and Karumba Basins.||||||
25817|Bulimba Formation|23510|5|Briefly described|Map Legend||Tertiary|||||||
25817|Bulimba Formation|23616|5|Briefly described|Table 1C p12, p40|||Unconformably overlies Proterozoic metamorphics and granitoids of the Dargalong Inlier. Karumba Basin.||||||
25817|Bulimba Formation|23713|5|Briefly described|p34|||Karumba Basin.||||||
25817|Bulimba Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
25817|Bulimba Formation|24073|5|Briefly described|p378 Table 2|Cenozoic|Cenozoic|Formerly part of Lynd Formation? Maximum thickness: 100m. Geological Province: Carpentaria Basin.||||||25-JUN-15
25817|Bulimba Formation|24485|3|Fully described|p2, p38 Tb.6|Eocene|Paleocene|Max Thickness: ~120m. Basal unit of the Karumba Basin. Geological Province: Karumba Basin.||||||25-JUN-15
25817|Bulimba Formation|24486|5|Briefly described|Map legend|Tertiary|Tertiary|||||||
25817|Bulimba Formation|30582|6|Mentioned|p7|||||||||
25817|Bulimba Formation|31163|4|Described|p247|||U.Cretaceous - L. Tertiary||||||
25817|Bulimba Formation|31165|5|Briefly described|Table 1|||||||||
25817|Bulimba Formation|31166|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous or Early Tertiary||||||
25817|Bulimba Formation|31168|4|Described|p14|||Also mention Table 2.||||||
25817|Bulimba Formation|32392|6|Mentioned|Map legend|Tertiary|Late Cretaceous|U.Cret.-Tertiary||||||
25817|Bulimba Formation|32393|6|Mentioned|Map legend|Tertiary|Late Cretaceous|U.Cret.-Tertiary||||||
25817|Bulimba Formation|32395|6|Mentioned|p6|||Stratigraphic Table||||||
25817|Bulimba Formation|32396|4|Described|p8|||U.Cret.-Tertiary||||||
25817|Bulimba Formation|32563|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous or Early Tertiary||||||
25817|Bulimba Formation|32705|5|Briefly described|p183|||Mention P181||||||
25817|Bulimba Formation|32706|4|Described|Table 1|||See also P8||||||
25817|Bulimba Formation|33150|4|Described|p8|||See also P13. U.Cret.-Tertiary.||||||
25817|Bulimba Formation|33151|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Upper Cret.-Tertiary||||||
25817|Bulimba Formation|33177|5|Briefly described|Table 1|||||||||15-JUL-04
25817|Bulimba Formation|33178|4|Described|p12|||||||||
25817|Bulimba Formation|33179|4|Described|Table 2|||||||||
25817|Bulimba Formation|33180|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Upper Cretaceous to Tertiary||||||
25817|Bulimba Formation|33181|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous or Early Tertiary||||||
25817|Bulimba Formation|33182|2|Defined|p193|early Tertiary|Late Cretaceous|Upper Cretaceous - Lower Tertiary||||||
25817|Bulimba Formation|33184|6|Mentioned|Map legend|early Pliocene|late Miocene|Late Miocene to Early Pliocene||||||
25817|Bulimba Formation|33185|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous to Early Tertiary||||||
25817|Bulimba Formation|33226|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Late Cretaceous or Tertiary||||||
25817|Bulimba Formation|33528|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Late Cretaceous or Tertiary||||||
25817|Bulimba Formation|33529|6|Mentioned|Map legend|early Pliocene|late Miocene|Late Miocene - Early Pliocene||||||
25817|Bulimba Formation|33772|4|Described|p17|||||||||
25817|Bulimba Formation|33773|4|Described|Table 1|||||||||
25817|Bulimba Formation|33882|4|Described|Table 1|||Mention P7,8,15||||||
25817|Bulimba Formation|33908|6|Mentioned|p595|||||||||
25817|Bulimba Formation|34811|6|Mentioned|p5|||||||||
25817|Bulimba Formation|35187|6|Mentioned|Table1|||||||||
25817|Bulimba Formation|35204|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|||||||
25817|Bulimba Formation|35220|4|Described|p17|||||||||
25817|Bulimba Formation|36012|6|Mentioned|p16|||||||||
25817|Bulimba Formation|36216|6|Mentioned|p211|||||||||
25817|Bulimba Formation|36228|6|Mentioned|Map legend|Eocene|Eocene|||||||
25817|Bulimba Formation|36229|6|Mentioned|Map legend|Eocene|Eocene|||||||
25817|Bulimba Formation|37603|6|Mentioned|p443|||||||||
25817|Bulimba Formation|37605|6|Mentioned|p382|||||||||
25817|Bulimba Formation|37607|5|Briefly described|p334|||See also P333 and Fig.5.||||||
25817|Bulimba Formation|39315|6|Mentioned|Fig.6|||||||||
25817|Bulimba Formation|39445|5|Briefly described|Table 14|||||||||
25817|Bulimba Formation|39687|6|Mentioned|Fig.5|||||||||
25817|Bulimba Formation|39917|6|Mentioned|Map legend|Tertiary|Late Cretaceous|Late Cretaceous-Tertiary||||||
25817|Bulimba Formation|40218|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous to Early Tertiary||||||
25817|Bulimba Formation|40659|6|Mentioned|p250|||||||||
25817|Bulimba Formation|41022|6|Mentioned|p280|||||||||
25817|Bulimba Formation|42186|6|Mentioned|p384|||||||||
25817|Bulimba Formation|42464|6|Mentioned|p8|||||||||
25817|Bulimba Formation|42637|5|Briefly described|p29|||||||||
25817|Bulimba Formation|42650|4|Described|p17|||||||||
25817|Bulimba Formation|42691|5|Briefly described|map legend|Cenozoic||||||||19-NOV-08
25817|Bulimba Formation|43060|4|Described|p60,Table 1c|||||||||
25817|Bulimba Formation|43083|5|Briefly described|p185|||Geological province: Karumba Basin. Fluviatile sand, gravel and clay deposits.||||||17-JUN-09
25817|Bulimba Formation|43110|5|Briefly described|p56|||Suggested Paleocene to Eocene age.||||||
25817|Bulimba Formation|43254|5|Briefly described|map legend||Tertiary|||||||
25817|Bulimba Formation|43285|5|Briefly described|Map Legend||Tertiary|||||||
25817|Bulimba Formation|43287|5|Briefly described|Map Legend||Paleogene|||||||07-NOV-08
25817|Bulimba Formation|43596|4|Described|p40-41, p39 Tb. 4|Tertiary|Late Cretaceous|Basal unit in the Karumba Basin. Unconformable on Rolling Downs Group in many areas but obscured or gradational in others. Fluvial deposits of poorly sorted + subrounded to subangular clayey sandstone; quartz gravel+cobble intebeds common towards base.||||||07-APR-15
25817|Bulimba Formation|43625|4|Described|p48|||||||||
25817|Bulimba Formation|43738|5|Briefly described|p7|||||||||
25817|Bulimba Formation|43740|6|Mentioned|Fig.5,p45|Tertiary|Late Cretaceous|||||||
25817|Bulimba Formation|43810|6|Mentioned|p208|Pleistocene|Pliocene|||||||
25817|Bulimba Formation|43820|5|Briefly described|Map Legend|Tertiary|Late Cretaceous|||||||
25817|Bulimba Formation|44246|5|Briefly described|Map Legend||Tertiary|||||||
25817|Bulimba Formation|44926|5|Briefly described|Map Legend||Tertiary|||||||
25817|Bulimba Formation|45145|6|Mentioned|p30|||||||||
25817|Bulimba Formation|45168|6|Mentioned|p6|||||||||
25817|Bulimba Formation|46802|6|Mentioned|p131|||||||||
25817|Bulimba Formation|46812|5|Briefly described|p241|||||||||
25817|Bulimba Formation|46872|6|Mentioned|p103|||||||||
25817|Bulimba Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
25817|Bulimba Formation|50595|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, conglomerate, claystone.||||||01-JUL-04
25817|Bulimba Formation|50627|5|Briefly described|Map legend|Paleogene|Late Cretaceous|Clayey quartz sandstone, commonly pebbly; pebbly clay-rich siltstone, mudstone; conglomerate.||||||25-JUN-15
25817|Bulimba Formation|60081|5|Briefly described|Map legend||Late Cretaceous|Poolry sorted clayey quartzose sandstone and granule conglomerate, pebbly in places, sandy claystone.  Age is Late Cretaceous or Tertiary?||||||
25817|Bulimba Formation|60087|5|Briefly described|Map legend|||Late Cretaceous or Tertiary in age.||||||
25817|Bulimba Formation|61155|5|Briefly described|p16|Eocene||Thin sediment sheets over large areas of Karumba Basin. In the Gulf of Carpentaria area. Age: ?Eocene. Geological Province: Western Cape York, Karumba Basin. ||||||
25817|Bulimba Formation|64820|4|Described|pS6 Fig. 4, pS9|Paleogene|Paleogene|Overlain by the Aurukun Surface; unconformably overlies the Rolling Downs Group. Quartzose sandstone, siltstone, coal (peat) beds, claystone (<10% quartz). Geological province: Weipa Sub-basin, Carpentaria Basin. Weathering profile is described in detail.||||||04-MAR-09
25817|Bulimba Formation|64821|5|Briefly described|pS29, pS33, pS40|Paleogene|Paleogene|Unconformably overlies the Rolling Downs Group. Weathered sediments associated with bauxite deposits.||||||02-FEB-09
25817|Bulimba Formation|64822|5|Briefly described|pS88, pS92, pS99|Paleogene|Paleogene|Together with underlying Rolling Downs Group, hosted the development of the Weipa bauxite deposit - composed of a transported blanket of bauxite overlying a lateritic weathering profile. Thickness: 15m. Fluvial quartzose sst/siltst; contains peat offshore.||||||25-JUN-15
25817|Bulimba Formation|67402|6|Mentioned|p176, p177, p180, p239|Longfordian|Longfordian|Karumba Basin. Aquifers are present in this formation. Deposited in a fluvial to paralic environment. Approximately 160m thick. Unsuitable reservoir for the storage of carbon dioxide.||||Unconformably overlies the Normanton Formation. Overlain by the Carl Creek and Gregory Downs Limestones.|Clayey quartzose sand, sandstone, granule conglomerate, siltstone and claystone.|
25817|Bulimba Formation|68345|5|Briefly described|Map legend.|Tertiary|Tertiary||||||White to pale grey or reddish-brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|68349|5|Briefly described|Map legend.|Tertiary|Tertiary|Karumba Basin.|||||White to pale grey or reddish-brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|68356|5|Briefly described|Map legend.|Tertiary|Tertiary|Karumba Basin.|||||White to pale grey or reddish-brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|68405|5|Briefly described|Map Legend|Neogene|Paleogene|Carpentaria and Karumba Basins.||||Unconformably overlies Gilbert River Formation.|White, poorly indurated clayey quartzose to feldspathic sandstone, poorly sorted granule conglomerate, and sandy claystone; commonly ferruginised.|24-AUG-15
25817|Bulimba Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
25817|Bulimba Formation|69599|5|Briefly described|p585, p601-602, p605, p650|Eocene|Paleocene|Basal unit in the Karumba Basin. Widely distributed. Capped by laterite and silcrete of the Aurukun Surface. One of the hosts of the world's largest deposit of bauxite, at Weipa on the west coast of Cape York. Up to 150m thick. Fluvial deposits. Unfossiliferous. Probably Palaeocene-Eocene. Formation of the bauxite discussed. McConachie and Dunster (1997) "synonymised these units [Louisa and Floraville Formations] into the Bulimba Formation".||||Is overlain conformably by the Wyaaba beds. Equivalent to the Weipa beds, Fairview Gravel and Louisa and Floraville Formations.|Claystone, quartzose sandstone, granule conglomerate, siltstone and minor coal. Has developed a typical lateritic profile containing loose, free-running pisoliths of bauxite with little or no matrix.|
25817|Bulimba Formation|71409|5|Briefly described|p1061|Neogene|Neogene|||||Overlies Rolling Downs Group.|Gravels, sands and clays deposited in broad fans.|
25817|Bulimba Formation|71792|5|Briefly described|p61-p62|Eocene|Eocene|Karumba Basin.||||Conformably overlain by the Wyaaba beds.|White to play grey or reddish brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|71849|6|Mentioned|p8, p195|Quaternary|Tertiary|||||||
25817|Bulimba Formation|71853|5|Briefly described|Map legend.|Eocene|Paleocene||||||White to pale grey or reddish brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|71854|5|Briefly described|Map legend.|Eocene|Paleocene||||||White to pale grey or reddish brown, poorly indurated, clayey quartzose to feldspathic sandstone, poorly sorted granule to (locally) pebble conglomerate and sandy claystone; commonly ferruginised.|
25817|Bulimba Formation|73144|6|Mentioned|p8|Paleogene|Paleogene|Karumba Basin. Partial aquifer.||||||
36283|Bull Creek Granite|23291|4|Described|p97 Tb. 3.11|Early Permian|Early Permian|Parent: Kangaroo Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
36283|Bull Creek Granite|23510|5|Briefly described|Map Legend||Early Permian|of Kangaroo Creek Supersuite.||||||
36283|Bull Creek Granite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Kangaroo Creek Supersuite.||||
74065|Bullaganang Supersuite|63748|5|Briefly described|p25-26|Early Permian|Early Permian|Includes the Bullaganang and Mingimarny Suites.||||||07-FEB-11
74065|Bullaganang Supersuite|70876|5|Briefly described|p80|||Donchak et al (2013) incorporated this Supersuite into the Stanthorpe Supersuite; the authors of this volume however, note significant age ranges of the incorporated Supersuites and thus suggest this issue be revisited.||||||
74065|Bullaganang Supersuite|71628|5|Briefly described|p5: 1-2, 7; p19:103|||Donchak et al. (2007). Now the Mount Bullaganang Supersuite.|||Bullaganang Granite.|||
36277|Bulleringa Volcanic Subgroup|23291|4|Described|p38, p93 Tb. 3.9|Late Carboniferous|Late Carboniferous|Formerly "Scardon Volcanics". Age: 289+/-2Ma. Thickness: >400m. Geological Province: Georgetown Region.||||||08-JUL-15
36277|Bulleringa Volcanic Subgroup|23510|5|Briefly described|Map Legend||Early Permian|of Scardons Volcanic Group.||||||
36277|Bulleringa Volcanic Subgroup|68405|5|Briefly described|Map Legend|Cisuralian|Late Carboniferous|Kennedy Province. Shown as two groups of (mostly unnamed) units; a Late Carboniferous group, including Duffers Creek Dacite, and an Early Permian? (~290 Ma) group, including Dickson Creek Rhyolite.|~ 290 Ma in part|Of the Scardons Volcanic Group.|Includes Dickson Creek Rhyolite, Duffers Creek Dacite, and 23 unnamed units.|Unconformably underlain by the Blackman Gap Complex. Older than Brodies Camp Supersuite. Shown as equivalent age to Warby Volcanic Subgroup.|Rhyolitic to dacitic ignimbrite, breccia, crystal tuff, lava, porphyritic andesite, volcaniclastic sediments.|
36277|Bulleringa Volcanic Subgroup|69593|5|Briefly described|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|289 +/- 2 Ma (SHRIMP U-Pb zircon).|Scardons Volcanic Group.|||Rhyolitic ignimbrites.|
36277|Bulleringa Volcanic Subgroup|71592|5|Briefly described|Appendix A.||||289+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
23436|Bullhead Granite|23511|5|Briefly described|Map Legend||Early Permian|Age: 293 +/- 1Ma.||||||
23436|Bullhead Granite|24086|6|Mentioned|p312 Fig. 1|||||||||
23436|Bullhead Granite|24213|5|Briefly described|p777|Permian|Permian|||||||
23436|Bullhead Granite|42304|3|Fully described|p29|Permian|Carboniferous|Not dated, age assumed. Reserved April 1988 by R.J. Bultitude||||||
23436|Bullhead Granite|43098|2|Defined|p33|Early Permian||Rb-Sr rock-muscovite age of 293+/-1Ma. No type area assigned.||||||
23436|Bullhead Granite|43625|5|Briefly described|p123, Appendix 6|||||||||
23436|Bullhead Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
23436|Bullhead Granite|50596|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Whypalla Supersuite.  Garnet-muscovite adamellite.||||||30-JUN-04
23436|Bullhead Granite|60425|4|Described|p276-7 Appdx.|Early Permian|Early Permian|Of Mount Pike Suite (Whypalla Supersuite). S-type. White to pink (altered), fine- to medium-gr.,even-gr.garnet-biotite-muscovite leucogranite; garnet+muscovite relatively common; aureole foliation+assoc'd folds dev'd in country rocks adjacent to contact||||||07-FEB-11
23436|Bullhead Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Pike Suite.||||
69551|Bullock Creek Granite|68405|5|Briefly described|Map Legend|Early Silurian|Early Silurian|Pama Province.||Of the White Springs Supersuite.|||Pink to grey, coarse-grained, muscovite granite and pegmatite.|
69551|Bullock Creek Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
38039|Bullrush Conglomerate|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Polymictic granule, pebble and cobble conglomerate: clasts of quartzite, quartz sandstone, quartz, chert, brown porphyritic rhyolite and claystone in lithic sand-granule matrix.||||||
38039|Bullrush Conglomerate|65337|3|Fully described|p9 Fig.5, p21, pp26-27.|Paleoproterozoic|Paleoproterozoic|East-central MOUNT DRUMMOND area. 50 - 500 m of mainly subaerial alluvial fan to fan delta deposits. Clasts suggest rapid erosion of a lower McNamara Group terrane.The puzzling apparent superposition of several contrasting facies may be due to faulting.||Unit in McNamara Group.||Unconformably overlies Top Rocky Rhyolite and Drummond Formation. Is overlain by Plain Creek Formation.|Polymict granule, pebble and cobble conglomerates, cross-bedded sandstone; stromatolitic chert and chert-clast conglomerate, fine-grained lithic sandstone and siltstone.|
38039|Bullrush Conglomerate|69433|4|Described|p18:2, 6, 9-10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 50-500m thick. Contains a variety of sedimentary structures, reflecting deposition in subaerial alluvial fans building out into marine waters.||McNamara Group.||Unconformably overlies Top Rocky Rhyolite and Drummond Formation. Is overlain conformably by Plain Creek Formation. Correlated with Shady Bore Quartzite.|Polymictic granule, pebble and cobble conglomerate, massive or crudely bedded, largely clast supported in a matrix of lithic sand to granules; alternating with white, silicified, fine- to very coarse-grained cross-bedded sandstone.|12-JUL-16
38039|Bullrush Conglomerate|69673|4|Described|p52 fig 42,p53|||Up to 500m thick. Deposited in subaerial alluvial fans.||McNamara Group|||Polymictic granule, pebble and cobble conglomerate, alternating with cross bedded sandstone with minor carbonate rocks and siltstone.|
38039|Bullrush Conglomerate|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin.||McNamara Group||Overlies Brumby Formation and underlies Shady Bore Quartzite.||
38039|Bullrush Conglomerate|72527|4|Described|p3, p8, p119-131, p193, p194, p197.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Previously included in Maloney Creek Formation, then Musselbrook Formation (both now obsolete). Up to 500 m thick. Uncertain  stratigraphic affinity.Two samples dated from conglomerate. Second sample is specifically rhyolite clasts: age 1723+/-6 Ma which confirms source as Top Rocky Rhyolite. Displays remarkably similar age spectra to Caulfield beds, Bowgan Sandstone, and Crow Formation. Type locality near sample site shown as 137.6299dE 18.43856dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios.|1646+/-5 Ma max dep age.|McNamara Group||Conformably overlain by Plain Creek Formation. Unconformably overlies Top Rocky Rhyolite. Shown as laterally equivalent to Shady Bore Quartzite.|Crudely bedded polymict granule, pebble to cobble conglomerate, with interbedded cross-bedded quartz and lithic sandstone, siltstone. Includes carbonate interbeds with relic stromatolites,  qtz, qtzite, ssst, chert, clayst, rhyolite clasts.|
38039|Bullrush Conglomerate|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Shown as being located in the Northern Territory part of the McNamara Group.||McNamara Group||Overlies and equivalent to Brumby Formation and underlies and equivalent to Shady Bore Quartzite.Partially laterally equivalent to Walford Dolomite and Fish River Formation.||
38039|Bullrush Conglomerate|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Equivalent to Shady Bore Quartzite and Plain Creek Formation.||
38039|Bullrush Conglomerate|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Overlain by Plain Creek Formation.||
23437|Bullseye Rhyolite|9531|5|Briefly described|Map Legend|Permian|Carboniferous|Rhyolitic ash tuff, ignimbrite, minor lava and agglomerate, sandstone, conglomerate, siltstone.||||||02-JUL-04
23437|Bullseye Rhyolite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Mount Little Volcanic Group. Overlies Croydon Volcanic Group. Age: >/-275Ma. Thickness: ~50m. Geological Province: Georgetown Region.||||||25-JUN-15
23437|Bullseye Rhyolite|23430|6|Mentioned|p499|||||||||
23437|Bullseye Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V4. I-Type.||||||
23437|Bullseye Rhyolite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
23437|Bullseye Rhyolite|40659|6|Mentioned|p250|||Mention P254||||||
23437|Bullseye Rhyolite|40860|4|Described|p109|||||||||
23437|Bullseye Rhyolite|40954|6|Mentioned|p132|||||||||
23437|Bullseye Rhyolite|43259|4|Described|Appendix 1,p1.||Permian|||||||
23437|Bullseye Rhyolite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province. Four facies associations are mapped separately.||Unit in Mount Little Volcanic Group.|||Conglomerate, sandstone, siltstone, rhyolitic crystal tuff, rhyolitic ignimbrite, breccia and lava, silicified wood locally at base, rhyolitic ash tuff, minor lava and breccia, tuffaceous sandstone.|
23437|Bullseye Rhyolite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province. Four facies associations are mapped separately.||Unit in Mount Little Volcanic Group.|||Conglomerate, sandstone, siltstone, rhyolitic crystal tuff, rhyolitic ignimbrite, breccia and lava, silicified wood locally at base, rhyolitic ash tuff, minor lava and breccia, tuffaceous sandstone.|
77682|Bulluburrah Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite?|||Greenish grey, fine-grained, very highly porphyritic hornblende-biotite monzogranite to granodiorite?; variably altered.|
24202|Bulmung Sandstone Member|22665|6|Mentioned|P227|||||||||
24202|Bulmung Sandstone Member|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Lawn Hill Formation.||||||07-NOV-08
24202|Bulmung Sandstone Member|23405|5|Briefly described|p567|||Of Lawn Hill Formation.||||||
24202|Bulmung Sandstone Member|23964|5|Briefly described|p1269 Table 1|||Of Lawn Hill Formation. Geological Province: Mount Isa Inlier.||||||
24202|Bulmung Sandstone Member|37459|2|Defined|p433|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
24202|Bulmung Sandstone Member|38237|6|Mentioned|p131|||||||||
24202|Bulmung Sandstone Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24202|Bulmung Sandstone Member|38310|6|Mentioned|p237|||||||||
24202|Bulmung Sandstone Member|38348|4|Described|p22|||||||||
24202|Bulmung Sandstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24202|Bulmung Sandstone Member|43652|6|Mentioned|Fig.15,p393|||||||||
24202|Bulmung Sandstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Lawn Hill Formation.||||||
24202|Bulmung Sandstone Member|45166|5|Briefly described|p30|||||||||
24202|Bulmung Sandstone Member|61904|5|Briefly described|p132 Fig. 2|Proterozoic|Proterozoic|Of Lawn Hill Formation.||||||
24202|Bulmung Sandstone Member|65337|6|Mentioned|p33.|||May be equivalent to uppermost sandstone unit in Plain Creek Formation.||Unit in Lawn Hill Formation.||||
24202|Bulmung Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Isa Superbasin. Appears as Bulmung Sandstone in the Mount Isa Block Time-Space Plot, and simply as Bulmung in the Eastern Australia Plot.|~1616 Ma.|Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base.|
24202|Bulmung Sandstone Member|69591|6|Mentioned|p43 Fig.2.31|||Isa Superbasin.||||||
24202|Bulmung Sandstone Member|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base.|
24202|Bulmung Sandstone Member|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base.|
24202|Bulmung Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base.|
24202|Bulmung Sandstone Member|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base.|
24202|Bulmung Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base|
24202|Bulmung Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base|
24202|Bulmung Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base|
24202|Bulmung Sandstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Flaggy to blocky, micaceous, lithic sandstone and conglomeratic sandstone, shale clasts common near base|
24202|Bulmung Sandstone Member|73144|6|Mentioned|p8|Statherian|Statherian|Isa Superbasin. Part of the Lawn Supersequence. Partial aquifer. Potential tight gas/oil. Base of Lawn Supersequence, although not base of Lawn Hill Formation.||Lawn Hill Formation, McNamara Group||||14-OCT-22
39029|Bundaleer Tonalite|23799|5|Briefly described|p117|||Of the Dumgree Suite.  Geological Province: Yarrol Province.||||||
39029|Bundaleer Tonalite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbb].  Pale grey, medium-grained leucocratic hornblende-biotite tonalite, minor pale pink medium-grained bioite granite.||||||
39029|Bundaleer Tonalite|50209|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||17-MAY-04
39029|Bundaleer Tonalite|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
39029|Bundaleer Tonalite|68008|2|Defined|p353 p355,p357, p359-361,p363,p366,p621|Early Triassic|Permian|New name, for deeply weathered granitic rocks which form most of the E lobe of Bouldercombe Igneous Complex. The southern part of the Bundaleer Tonalite was referred to as Moonmera Granite (Staines, 1952,1953; The Staff, Mount Morgan Limited, 1965); this latter name is restricted to the Moonmera Porphyritic Granodiorite 7km N of Mount Morgan. Forms a NE-trending belt 16 x 8km from the Razorback Range. Named after the old railway siding of Bundaleer; the type area is the series of cuttings along the abandoned Mount Morgan to Kabra railway line up the Razorback Range. Lack of outcrop conceals relationship with Gavial Gabbro. Geophysics briefly described and modelled. Similar geochemistry to Dumgree Tonalite. K-Ar biotite ages by Ford et al. (1976) and Webb and McDougall (1968) respectively. Other, similar ages given. Appears as Bundaleer Granodiorite on p330 and p334.|264 +/- 5 Ma; 242 +/- 5 Ma (recalculated).|Bouldercombe Igneous Complex.||Intrudes Capella Creek Group, Mount Alam Formation and ? Gracemere Gabbro. Is overlain by Precipice Gabbro. Is intruded by Moonmera Porphyritic Granodiorite and Kabra Quartz Monzodiorite.|Pale grey, medium-grained, leucocratic hornblende-biotite tonalite. Altered rocks in the eastern margin are almost pure white.|
39029|Bundaleer Tonalite|68679|4|Described|p424, p426-427|||Yarrol Province. NE-trending, ~16 x 8 km intrusion. Most extensive unit in the Complex: forms the core of the eastern lobe. Is surrounded by a rim consisting of Gracemere, Gavial and Quarry Gabbros. Geochemistry briefly described. Other age determinations ranging to c.243 Ma are given.|263 +/- 5 Ma (Green, 1975).|Bouldercombe Igneous Complex.||Intrudes Capella Creek Group, Mount Alma Formation, Gracemere Gabbro. Is intruded by Moonmera Porphyritic Granodiorite and (possibly) Kabra Quartz Monzodiorite.|Leucocratic hornblende-biotite tonalite.|
27077|Bundock Creek Group|22800|5|Briefly described|Fig.14 p592|Visean|Frasnian|||||||
27077|Bundock Creek Group|23032|4|Described|p30,53|Carboniferous|Late Devonian|||||||
27077|Bundock Creek Group|23291|4|Described|p37, p81 Tb. 3.6|Carboniferous|Late Devonian|Geological Province: Georgetown Region.||||||25-MAR-08
27077|Bundock Creek Group|23424|5|Briefly described|Table 8.1 Fig 8.3 p336.|Early Carboniferous|Devonian|Was Bundock Creek Formation by White (1965). Lang et al (1989) raised Formation to Group status. Geological Province Bundock Basin. Max thickness 6000 m.||||||
27077|Bundock Creek Group|23430|4|Described|p478-479|||Also see p506. Underlying Unit Broken River Group - unconformable. Bundock Basin Province.||||||
27077|Bundock Creek Group|23431|5|Briefly described|p541|||Bundock Basin||||||
27077|Bundock Creek Group|23522|5|Briefly described|p250 Fig 6||Frasnian|||||||
27077|Bundock Creek Group|23619|5|Briefly described|p17|||Graveyard Creek Subprovince.||||||
27077|Bundock Creek Group|24399|5|Briefly described|p280|Late Devonian|Middle Devonian|Geological Province: Broken River Province.||||||
27077|Bundock Creek Group|24577|4|Described|p751, p754 Fig. 2|Early Carboniferous|Late Devonian|Maximum thickness: >6 km. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
27077|Bundock Creek Group|24613|5|Briefly described|p6 Fig. 3, p133|Early Carboniferous|Late Devonian|Contains Teddy Mount and Boroston Formations, and the Rockfields Member within one of its units. Geological province: Broken River Province. Presented as upper and lower Bundock Creek Group in Fig. 3.||||||07-FEB-11
27077|Bundock Creek Group|24614|4|Described|p191 Fig. 1, p202|||Includes the Bulgeri and Turrets Formations. Geological Province: Broken River Province.||||||07-FEB-11
27077|Bundock Creek Group|40961|3|Fully described|p242|||||||||
27077|Bundock Creek Group|41260|3|Fully described|p77|||Formerly Bundock Creek Formation. See also p97, p107 and Fig.18.||||||25-MAR-08
27077|Bundock Creek Group|41675|6|Mentioned|p71|||||||||
27077|Bundock Creek Group|41679|6|Mentioned|p251|||||||||
27077|Bundock Creek Group|41719|6|Mentioned|p213|||||||||
27077|Bundock Creek Group|41739|1|Redefined|p299|Early Carboniferous|Late Devonian|||||||
27077|Bundock Creek Group|42031|5|Briefly described|Fig.4 P761|||||||||
27077|Bundock Creek Group|42054|6|Mentioned|p273|||||||||
27077|Bundock Creek Group|42279|6|Mentioned|Fig.2 P18|||||||||
27077|Bundock Creek Group|42692|5|Briefly described|map legend|Devonian||||||||
27077|Bundock Creek Group|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27077|Bundock Creek Group|42709|6|Mentioned|map legend|||||||||
27077|Bundock Creek Group|42752|5|Briefly described|p47|||see also Fig.3 P47||||||
27077|Bundock Creek Group|42933|3|Fully described|p129, Fig.12|||||||||
27077|Bundock Creek Group|43113|6|Mentioned|p31|||||||||
27077|Bundock Creek Group|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27077|Bundock Creek Group|43603|5|Briefly described|p9|Carboniferous|Late Devonian|||||||
27077|Bundock Creek Group|43664|6|Mentioned|p77||Early Carboniferous|||||||
27077|Bundock Creek Group|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes: Harry Creek Formation, Boroston Formation, Teddy Mount Formation, Turrets Formation, Bulgeri Formation.||||||
27077|Bundock Creek Group|60705|6|Mentioned|p649|||||||||
27077|Bundock Creek Group|61727|5|Briefly described|p942 Fig.1|Early Carboniferous|Devonian|Geological Province: Broken River Province/Camel Creek Subprovince. See also p952||||||21-APR-06
27077|Bundock Creek Group|63154|5|Briefly described|p281 Fig. 3|Early Carboniferous|Late Devonian|Geological province: Broken River Province/Graveyard Creek Subprovince||||||11-APR-07
27077|Bundock Creek Group|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Comprises Bulgeri, Turrets, Teddy Mount, Boroston and Harry Creek Formations. Sandstones, siltstones, conglomerates, mudstones; some reworked tuff.||||||20-JUN-13
27077|Bundock Creek Group|65214|6|Mentioned|p280, p282|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27077|Bundock Creek Group|67402|6|Mentioned|p244|||Bundock Basin. Up to 6000m thick. ||||Disconformably overlies the Broken River Group.||
27077|Bundock Creek Group|67848|5|Briefly described|p3 Fig.2.|Early Carboniferous|Late Devonian|Extensional cover succession over the collisional accretion succession.||||||
27077|Bundock Creek Group|68336|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.|||Includes Bulgeri, Turrets, Teddy Mount, Boroston and Harry Creek Formations.|||
27077|Bundock Creek Group|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.|||Includes Bulgeri, Turrets, Teddy Mount, Boroston and Harry Creek Formations.|||
27077|Bundock Creek Group|68341|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.|||Includes Bulgeri, Turrets, Teddy Mount, Boroston and Harry Creek Formations.|||
27077|Bundock Creek Group|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.|||Includes Harry Creek, Boroston, Teddy Mount, Turrets and Bulgeri Formations.|||
27077|Bundock Creek Group|68478|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.|||Includes Bulgeri Formation, Turrets Formation, and Teddy Mount Formation.||Fluvial, lacustrine and minor marine sedimentary and felsic volcanic rocks.|
27077|Bundock Creek Group|68479|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.|||Includes Bulgeri Formation, Turrets Formation, and Teddy Mount Formation.||Fluvial, lacustrine and minor marine sedimentary and felsic volcanic rocks.|
27077|Bundock Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Broken River Province.||||||
27077|Bundock Creek Group|69030|5|Briefly described|p6, p15, p40|Carboniferous|Devonian|Bundock Basin (Broken River Province).||Bulgeri, Turrets, Teddy Mount, Boroston, Harry Creek Formations.||||
27077|Bundock Creek Group|69079|6|Mentioned|p5|Early Carboniferous|Devonian|Graveyard Creek Subprovince, Broken River Province.||||||
27077|Bundock Creek Group|69592|5|Briefly described|p251 Fig.4.35, p258-259, p267, p272-273|Mississippian|Devonian|See also p277, p297-298. Withnall et al. (1988). Bundock Basin, Broken River Province. Fills the Basin: up to 6km thickness of fluviatile, deltaic and shallow-marine sediments. Deformation described.|||Bulgeri, Turrets, Teddy Mount, Boroston, Harry Creek Formations.|Unconformably overlies Mytton Formation (Broken River Group).||
27077|Bundock Creek Group|69593|5|Briefly described|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.|||Harry Creek Formation.|||
27077|Bundock Creek Group|73147|6|Mentioned|p131|||||||||
27077|Bundock Creek Group|73201|6|Mentioned|p610, p620|Carboniferous|Late Devonian|Broken River Province. Contains conodonts[?].||||||
79371|Bungobine Rhyolite|70740|4|Described|i, iv, p87, p99, p115-p118|||Drummond Basin. Name derived from the Bungobine Holding where this unit outcrops extensively. Outcrop characteristics and distribution discussed. A type locality is mentioned and very briefly described.||Bulgonunna Volcanic Group||Overlies the Bimurra Volcanics. Overlain by the Whitestone Creek Dacite and Yacamunda Creek Dacite.|Moderately to strongly flow banded, aphanitic to weakly porphyritic coherent rhyolitic lavas and autobreccias.|
38279|Bungulla Monzogranite|23811|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Of Moonbi Plutonic Suite.  Very coarse-grained porphyritic monzogranite; large euhedral, pink K-feldspar in medium-grained matrix of plagioclase, quartz, K-feldspar, biotite, hornbledne and sphene; rounded, mafic enclaves abundant in places.||||||20-DEC-04
38279|Bungulla Monzogranite|23812|4|Described|p21 Tb.2, p30|Early Triassic|Late Permian|Of Moonbi Plutonic Suite.  Intruded by the Stanthorpe Monzogranite.||||||
38279|Bungulla Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Pale pinkish grey to grey, fine- to medium-grained (groundmass) , coarsely porphyritic titanite-hornblende-biotite monzogranite to granodiorite?; +pale pink to white K-feldspar megacrysts; locally granophyric; minor aplitic leucogranite; high magnetic res||||||12-DEC-07
38279|Bungulla Monzogranite|63748|3|Fully described|p81-82 Appdx.1 |||Of Bungulla Suite. Incl.in Undercliffe Falls Adamellite by Thomson (1976). Intruded by Stanthorpe + Ruby Ck Granites. Characterised by presence large euhedral K-feldspar phenocrysts + grains of titanite. I-type. See also p36, p41, p27 Fig. 27, p29 Fig. 33||||||07-FEB-11
38279|Bungulla Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Olenekian||248 - 243 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
38279|Bungulla Monzogranite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Dormans Flat, Ruby Creek, Sailor Jack and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
38279|Bungulla Monzogranite|68679|5|Briefly described|p453, p455-456, p458, p460-461, p464|Middle Triassic|Permian|Northern New England Batholith. Previously the Bungulla Porphyritic Adamellite of Shaw (1969). ~18 km2. Extends from Wallangarra into NSW. A relatively mafic unit. Geochemical plots.||Bungulla Suite.||Possibly intrudes the Wallangarra Volcanics. Is intruded by Stanthorpe and Ruby Creek Granites.|Pinkish-grey, coarsely porphyritic titanite-hornblende-biotite granodiorite? to monzogranite; K-feldspar phenocrysts; locally rapakivi textured, mafic enclaves, granophyric; relatively mafic. Oxidised, highly evolved, high-K; I-type.|
38279|Bungulla Monzogranite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
38279|Bungulla Monzogranite|69639|4|Described|p1-p2, p5, p8-p9, p50, p62|Lopingian|Lopingian|New England Orogen. Contact with the Billyrimba Leucomonzogranite is obscured by poor outcrop. Said to be of the Bolivia Range Suite on p80. Sampling locality, petrography and geochronology are discussed. Geochemically similar to the Bookookoorara Monzogranite. Mistakenly referred to as the Bungulla Granite on p9, p81, p240. See also p80-p86, p157, p163, p221, p240.|252.5 +/- 1.2 Ma (SHRIMP)|Bungulla Suite||Intruded by the Mount Jonblee Leucomonzogranite. Intrudes the Sandy Flat Monzogranite.|Coarse-grained, porphyritic biotite-amphibole bearing monzogranite.|
38279|Bungulla Monzogranite|70217|5|Briefly described|p74 tbl 14.1|Changhsingian|Changhsingian|New England Orogen.|252.5 +/- 1.2 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
38279|Bungulla Monzogranite|71628|3|Fully described|p1:7; p7: 1, 37; p8:80; p11: 2, 7-15, 19|||See also p11: 24, 26, 35, 40, 45; p12: 4-5; p14: 12, 28; p15: 5, 16, 25, 33, 57, 65, 82, 92-93, 105; p16-20; p19: 18, 21-22, 94, 97, 160. Willis (1987). Previously the Bungulla Porphyritic Adamellite (Wilkinson,1969) after Bungulla Porphyritic-Adamellite (Shaw, 1964?); later Bungulla Adamellite (Robertson, 1970) and 'Bungulla Porphyritic Adamellite' (Thomson, 1976, with other, often informal, variations). The history of its varied and current definitions is detailed. Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Apparently previously included rocks here grouped as the Sailor Jack Supersuite. Named after the locality of Bungulla. Type locality is 8 km S of Tenterfield along the New England Highway. Comprises three bodies (described), bounded by numerous units (all named). Forms gently undulating country with outcrops of isolated tors and whalebacks. Described in great detail. Geochemistry described. RELATED UNITS (continued): Is 'bound' (?intruded) by Cottesbrook Monzogranite and Billyrimba Leucomonzogranite. Is faulted against Stanthorpe and Rocky River Monzogranites. Is intruded by Mount Jonblee Leucomonzogranite, Ruby Creek Leucogranite, Black Snake Creek Granite and Mount Lindesay Monzogranite. Abuts Tenterfield Creek Leucosyenogranite.|252.5 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Bungulla Suite.||Intrudes Dundee Rhyodacite, Wallangarra Volcanics, Sandy Flat Leucomonzogranite and undifferentiated Wandsworth Volcanic Group. See COMMENTS for more.|Coarsely porphyritic, biotite-hornblende-(clinopyroxene) monzogranite characterised by large pink K-feldspar megacrysts set in a medium-grained matrix; locally contains abundant enclaves. I-type.|
38279|Bungulla Monzogranite|72528|5|Briefly described|p78, p109.|Lopingian|Lopingian|Age determined on the Kangaroo Swamp mass, Chisholm et al (2014). It is the Bungulla mass of this unit that is intruded by the Black Snake Creek Granite.|252.5+/-1.2 Ma U-Pb SHRIMP.|||Intruded by Black Snake Creek Granite||
67899|Bungulla Suite|61783|5|Briefly described|p296|||In the Tenterfield area.  Granites.||||||
67899|Bungulla Suite|63748|5|Briefly described|p35, p36|||Includes the Bungulla and Undercliffe Falls Monzogranites and part of Bookookoorara Monzogranite. I-type granites occur mainly scattered around eastern margins of the Stanthorpe Granite.||||||07-FEB-11
67899|Bungulla Suite|68679|5|Briefly described|p456, p458-461, p462 Fig.5.133, p464|||See also p465 Fig.5.143. Northern New England Batholith. Forms scattered remnant intrusions around the southern margins of the spatially-associated Stanthorpe Granite. Geochemistry plots, discussion.||Stanthorpe Supersuite.|Bungulla Monzogranite.|||
67899|Bungulla Suite|69639|5|Briefly described|p9, p157|||New England Orogen.||Stanthorpe Supersuite|Includes the Bungulla Monzogranite and the Bookookoorara Monzogranite.|||
67899|Bungulla Suite|71628|5|Briefly described|p8: 97; p11:1-2, 5, 11-12,26,40; p19-21|||Donchak et al. (2007). Northern New England Batholith. In this study it broadly corresponds to Bungulla Supersuite.||Bungulla Supersuite.|Bungulla, Undercliffe Falls Monzogranites.|||
28044|Bunira Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
28044|Bunira Granite|22781|4|Described|p31|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
28044|Bunira Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes the Holroyd Group and Peringa Tonalite||||||
28044|Bunira Granite|43596|5|Briefly described|p27 Tb. 3, p36|||Of Ebagoola Suite (Kintore Supersuite). Mapped as Kintore Adamellite by Willmott et al (1973). Intrudes Sugarbag Creek Quartzite and Dinah Formation. Pale grey equigranular muscovite-biotite granite.||||||27-JAN-09
28044|Bunira Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
29999|Bunk Creek Granite|23423|5|Briefly described|p311 Table 7.4||Late Permian|I-type granite. Pieter Botte Supersuite.||||||
29999|Bunk Creek Granite|43070|2|Defined|p37|Late Permian||Of Yates Supersuite.||||||07-OCT-08
29999|Bunk Creek Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Pieter Botte Supersuite.||||||06-JUL-04
29999|Bunk Creek Granite|60425|5|Briefly described|p51 Tb. 3, p54 Tb. 4, p272-3 Appdx. 1|Late Permian|Early Permian|Of Nulbullul Suite (Pieter Botte Supersuite). Intruded and hornfelsed Obree Point Volcanics. Also intruded Hodgkinson Fm. I-type, biotite granite, moderately to highly porphyritic, fine- to medium-grained -- further lithological details included (p273).||||||07-FEB-11
29999|Bunk Creek Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Nulbullulul Suite.||||
23443|Bunkers Hill Granite|22847|3|Fully described|p 43|||||||||
23443|Bunkers Hill Granite|23504|5|Briefly described|Map Legend||Ordovician|||||||
23443|Bunkers Hill Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 103. Assumed to be I-Type.||||||
23443|Bunkers Hill Granite|42245|2|Defined|p32|Ordovician||||||||
23443|Bunkers Hill Granite|43093|4|Described|Appendix 1||Early Ordovician|Probable Early Ordovician||||||
23443|Bunkers Hill Granite|43259|4|Described|Appendix 1,p22.||Ordovician|||||||
23443|Bunkers Hill Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
23443|Bunkers Hill Granite|43936|5|Briefly described|Map Legend||Ordovician|||||||
77877|Burangoo Sandstone|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Paleoproterozoic|South Nicholson Basin. Detrital [?zircon] ages: 1600 +/-21 Ma (Magee et al, in prep).||South Nicholson Group|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles to 1cm; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|67539|5|Briefly described|p14|||North of the Elizabeth Creek fault. Raised to formation rank.||Of the South Nicholson Group.||Overlain by the Wallis Siltstone. Underlain by the Pandanus Siltstone.||
77877|Burangoo Sandstone|68146|4|Described|p2, p6, p20-27, p29, p196-197, p211|||South Nicholson Region. Also given 1591 +/- 10 Ma MDA from rocks mistakenly thought to have been Constance Sandstone. Whole-rock Sm-Nd isotopic data tabulated.|1565 +46/-45 Ma max. deposition age.|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|White to,light grey, thick-bedded, mainly fine- to medium-grained felspathic quartz sandstone; some coarser-grained laminae; cross-bedded.|
77877|Burangoo Sandstone|68575|4|Described|p3, p6-7, p18-26, p125, p128|||South Nicholson Basin. Formerly part of Constance Sandstone. Shows significantly different provenance from that of Hedleys Sandstone.|1602 +/- 30 Ma (maximum depositional age).|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|Thick-bedded, cross-bedded, fine- to very coarse-grained quartz sandstone with scattered granules and laminae of granules.|
77877|Burangoo Sandstone|69591|4|Described|p52-54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Predominantly fluvial. Another MDA given is 1600 +/- 21 Ma.|1566 +/- 46 Ma (MDA: Carson et al., 2011).|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|Thick-bedded, medium- to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles to 1cm; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|71369|3|Fully described|p1, p6, p8-9, p12-19, p47-49|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Previously (Roberts et al., 1963) undifferentiated Constance Sandstone; later (Rawlings et al., 2008) the Burangoo Sandstone Member of Constance Sandstone. Upgraded in this study (Sweet, 2017) to Formation status. 50-320m thick. The type section is near Burangoo Waterhole on the Nicholson River, where it is 320m thick. Mainly fluvial deposits.||Wild Cow Subgroup.||Overlies Pandanus Formation ?unconformably and Lawn Hill Formation locally. Is overlain by Wallis Formation and locally by Schultz Sandstone Member.|Basal white to light-grey, thick- and very thick-bedded, fine- to medium-grained quartz sandstone; coarsening-up to very coarse grained and granule-rich sandstone, before fining-upwards to fine- to medium-grained sandstone.|
77877|Burangoo Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1566 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
77877|Burangoo Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Wallis Formation. Underlain by Pandanus Formation.|Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Wallis Formation. Underlain by Pandanus Formation.|Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72526|5|Briefly described|p8 Fig.1.3|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||?Wild Cow Subgroup, South Nicholson Group||Overlies Pandanus Formation and underlies Wallis Formation.||
77877|Burangoo Sandstone|72527|5|Briefly described|p41|||Elevated to Formation-level in Qld, within the older Wild Cow Subgroup (Sweet, 2017). See also Burangoo Sandstone Member (as used in NT).||Wild Cow Subgroup||||
77877|Burangoo Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|See also misspelling 'Bunangoo Sandstone' on p33 Fig.12. Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Pandanus Formation and underlies Wallis Formation.||
77877|Burangoo Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in QLD. Distinct from Burangoo Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77877|Burangoo Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Pandanus Formation. Overlain by Wallis Formation.||
77877|Burangoo Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Pandanus Formation. Overlain by Wallis Formation.||
25820|Burdekin Formation|23422|5|Briefly described|p180, p206 Table 6.3|Middle Devonian|Middle Devonian|Of Fanning River Group.||||||
25820|Burdekin Formation|23430|5|Briefly described|Plate 14.11 + p505||Devonian|In the Burdekin Basin Province.||||||14-NOV-07
25820|Burdekin Formation|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of Fanning River Group.||||||14-NOV-07
25820|Burdekin Formation|23893|5|Briefly described|p16|Middle Devonian|Middle Devonian|Of Fanning River Group.  Geological Province: Burdekin Basin.||||||
25820|Burdekin Formation|24610|6|Mentioned|p63|Givetian|Emsian|Geological Province: Burdekin Basin. The name Burdekin Limestone is preferred by the authors of this study.||||||
25820|Burdekin Formation|24611|5|Briefly described|p193|Givetian|Eifelian|Geological Province: Burdekin Basin.  See also p196 Fig. 2.||||||
25820|Burdekin Formation|24612|4|Described|p10|Givetian|Eifelian|Of the Fanning River Group. Geological Province: Burdekin Basin. Thickness: 500 m. Predominantly limestone and siltstone, with coral associations. Interfingers with Big Bend Arkose.||||||14-NOV-07
25820|Burdekin Formation|24613|2|Defined|p9 Fig. 4, p16-17, Tb. 1|Eifelian|Eifelian|Of Fanning Gp. Conformable over Big Bend Arkose; gradational up into Cultivation Gully Fm. Max.thickness: 520m (variable). Geol.prov: Burdekin Basin. Fossiliferous l'st (dominated by corals, stromatoporoids), minor silts.+ sst. Detailed lithology incl.||||||15-MAY-15
25820|Burdekin Formation|24614|6|Mentioned|p192|||Name offered as an alternative for Burdekin Limestone.||||||07-FEB-11
25820|Burdekin Formation|30814|6|Mentioned|p71|||||||||
25820|Burdekin Formation|31285|4|Described|p81|||See also p84, 88. Givetian. Unit of Fanning River Group.||||||14-NOV-07
25820|Burdekin Formation|31999|5|Briefly described|p140|||See also Table 11||||||
25820|Burdekin Formation|32140|6|Mentioned|p5|||||||||
25820|Burdekin Formation|32619|6|Mentioned|p463|||Givetian. Fauna||||||
25820|Burdekin Formation|35008|5|Briefly described|p179|||||||||
25820|Burdekin Formation|37573|4|Described|Table 1|||||||||
25820|Burdekin Formation|39445|5|Briefly described|Table 5|||||||||
25820|Burdekin Formation|39686|5|Briefly described|Table 1|||||||||
25820|Burdekin Formation|39731|6|Mentioned|p31|||||||||
25820|Burdekin Formation|39732|6|Mentioned|p29|||||||||
25820|Burdekin Formation|42295|5|Briefly described|Fig.2 P5|||||||||
25820|Burdekin Formation|42689|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
25820|Burdekin Formation|42690|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
25820|Burdekin Formation|43095|5|Briefly described|Plate 2|||Of Fanning River Group.||||||14-NOV-07
25820|Burdekin Formation|43461|14|Not recorded|table p618||Givetian|Part of Fanning River Group||||||
25820|Burdekin Formation|43530|14|Not recorded|p1037|||||||||
25820|Burdekin Formation|43933|5|Briefly described|Map Legend||Middle Devonian|Of Fanning River Group.||||||14-NOV-07
25820|Burdekin Formation|43935|5|Briefly described|Map Legend||Middle Devonian|Of Fanning River Group.||||||22-FEB-05
25820|Burdekin Formation|44058|14|Not recorded|p102-3,Tb.p104|||Part of Fanning River Group.||||||
25820|Burdekin Formation|44061|14|Not recorded|p10||Devonian|formation of Fanning River Group.||||||
25820|Burdekin Formation|44091|14|Not recorded|p31,Tb. 3|||Basal formation of Fanning River Group.||||||
25820|Burdekin Formation|44516|14|Not recorded|p31|||See also Lexicon.||||||
25820|Burdekin Formation|44583|2|Defined|p147|||See also Lexicon.||||||
25820|Burdekin Formation|45009|14|Not recorded|p7||Middle Devonian|Ref. to Jack 1889||||||
25820|Burdekin Formation|48904|2|Defined|p23|Givetian|Givetian|||||||
25820|Burdekin Formation|62522|6|Mentioned|p28|||Overlain by undifferentiated Dotswood Group rocks. Geological Province: Burdekin Basin.||||||13-NOV-07
25820|Burdekin Formation|63118|6|Mentioned|p202|||Its fauna is correlated with that of Moore Creek area.||||||13-MAR-07
25820|Burdekin Formation|65940|6|Mentioned|p201|Givetian|Givetian|Contains Endophyllum columna, ascribed mid-Givetian age (Zhen and Jell 1996).||||||
25820|Burdekin Formation|67402|4|Described|p239, p247, p248|Givetian|Givetian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under marine (inner-distal shelf) conditions. ||Fanning River Group||Overlies the Big Bend Formation. Overlain by the Cultivation Gully Formation.|Variable, highly fossiliferous carbonate rocks including calcareous sandy siltstones, pellet grainstones, wackestones, mudstones, coralline packstones, crinoidal grainstones and biostromal units.|
25820|Burdekin Formation|68350|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Burdekin Basin.||Unit in Fanning River Group.||Is overlain conformably by Vanneck Formation.|Fossiliferous limestone (calcirudite, calcarenite and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone; fossils dominated by corals and stromatoporoids.|
25820|Burdekin Formation|68351|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Burdekin Basin.||Unit in Fanning River Group.||Is overlain conformably by Vanneck Formation.|Fossiliferous limestone (calcirudite, calcarenite and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone; fossils dominated by corals and stromatoporoids.|
25820|Burdekin Formation|68419|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Of the Burdekin Basin. The three facies are mapped separately.||Of the Fanning River Group.||Conformably overlain by the Vanneck Formation, Dotswood Group.|Fossiliferous limestone (calcirudite, calcarenite, and lesser calcilutite), minor sandy limestone, calcareous sandstone and mudstone, fossils dominated by corals and stromatoporoids; basal red polymictic conglomerate; and undivided.|
25820|Burdekin Formation|68420|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Of the Burdekin Basin.||Of the Fanning River Group.||Conformably overlain by the Vanneck Formation, Dotswood Group.|Fossiliferous limestone (calcirudite, calcarenite, and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone; fossils dominated by corals and stromatoporoids.|
25820|Burdekin Formation|68576|5|Briefly described|Q_11: p43|Middle Devonian|Middle Devonian|Townsville area. Previously quarried for lime and cement manufacture.|||||Limestone.|
25820|Burdekin Formation|68731|5|Briefly described|p177 Fig 3.91, p183, p185 Tb 3.4, p186|Middle Devonian|Middle Devonian|Cook (1995). Burdekin Basin. < 520 m thick. Depositional environment discussed. Contains diverse rugose and tabulate corals and stromatoporoids; also brachiopods, molluscs, crinoids.||Of the Fanning River Group.|||Comprises calcilutite with a variable siliciclastic component and nodular in parts, minor calcareous arkosic sandstone, stromatoporoid biostrome and local development of boundstone, framestone and bioherms. Rare crinoidal grainstone.|
25820|Burdekin Formation|69030|5|Briefly described|p6|Devonian|Devonian|Camel Creek Subprovince (Broken River Province).||Fanning River Group.||||
25820|Burdekin Formation|73143|6|Mentioned|p11, p18|Givetian|Givetian|Burdekin Basin. Lower Givetian age. Contains Aphyllum, Neomphyma and Spongophyllum species of rugose coral.||||||
26256|Burges Formation|23032|5|Briefly described|p27 fig6|Devonian|Devonian|||||||
26256|Burges Formation|23424|5|Briefly described|Table 8.1 p336.|Givetian|Emsian|Of Wando Vale Subgroup/Broken River Group, Graveyard Creek Subprovince.||||||
26256|Burges Formation|23430|5|Briefly described|p505|||||||||
26256|Burges Formation|24613|6|Mentioned|p131|||Geological province: Broken River Province. Referred to as lower Burgess Formation.||||||07-FEB-11
26256|Burges Formation|41260|4|Described|Table 1|||||||||
26256|Burges Formation|41679|2|Defined|p257|Givetian|Emsian|Age: Emsian to early Givetian.||||||
26256|Burges Formation|41719|6|Mentioned|Fig.2|||||||||
26256|Burges Formation|41739|6|Mentioned|Fig.2|||||||||
26256|Burges Formation|41740|6|Mentioned|p222|||||||||
26256|Burges Formation|42031|5|Briefly described|Fig.5 P762|||||||||
26256|Burges Formation|42054|6|Mentioned|p273|||||||||
26256|Burges Formation|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
26256|Burges Formation|42709|6|Mentioned|map legend|||||||||
26256|Burges Formation|42933|3|Fully described|Table 2|||See also p116.||||||
26256|Burges Formation|50093|3|Fully described|p237, p329 Fig.2, p334-338|Givetian|Emsian|Polymictic conglomerate and sandstones. Three lithofacies (mudrocks, carbonates and clastics) decribed in detail. Of Broken River Group.||||||24-JAN-13
26256|Burges Formation|68298|5|Briefly described|p224|Givetian||Limestone lithofacies range from Eifelian age (J.S. Jell, pers. comm) into early Givetian (Withnall et al., 1988).||||||24-JAN-13
26256|Burges Formation|68336|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Calcareous mudstone with lesser calcareous fine- to medium-grained arenite, polymictic conglomerate (with some large limestone clasts) and limestone.|
26256|Burges Formation|68341|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Calcareous mudstone with lesser calcareous fine- to medium-grained arenite, polymictic conglomerate (with some large limestone clasts) and limestone.|
26256|Burges Formation|68478|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Calcareous mudstone with lesser calcareous fine to medium-grained arenite, polymictic conglomerate (some with large limestone clasts) and limestone.|
26256|Burges Formation|68479|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Calcareous mudstone with lesser calcareous fine to medium-grained arenite, polymictic conglomerate (some with large limestone clasts) and limestone.|
26256|Burges Formation|69592|3|Fully described|p259, p264-267|Middle Devonian|Early Devonian|Wade Anticlinorium; Graveyard Creek Subprovince, Broken River Province. Apart from its Member, this Formation has four lithofacies (detailed). Deposited in a broad (10-20km across) submarine channel dividing carbonate shelves to the N and S. Contains Emsian-Eifelian conodonts.||Wandovale Subgroup.|Phar Lap Member.|Overlies Jack Formation; variously overlies Shield Creek Formation. Is overlain by Lomandra Formation. Lateral equivalent of Dosey Limestone. Interfingers with Wandovale Subgroup.|Polymict conglomerate-calcirudite-sandstone intervals; mudstone-limestone-sandstone intervals; limestone lenses up to 50m thick and 5km long; intervals of mudstone-sandstone.|
29316|Burke Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29316|Burke Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 316. I-Type.||||||
29316|Burke Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29316|Burke Granite|43087|6|Mentioned|p53|||Reserved as Burke Adamellite.||||||
29316|Burke Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite. (Ootann Supersuite).  Pale grey to pink, medium to coarse, biotite granite.||||||15-JUN-06
29316|Burke Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|Late? Carboniferous in age.||||||
29316|Burke Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pale grey to pink, medium- to coarse-grained biotite granite.||||||07-FEB-11
29316|Burke Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pale pink, medium-grained, porphyritic (hornblende-titanite-)biotite monzogranite; cut by leucogranite dyke(s).|
37808|Burlington Granite|23291|5|Briefly described|p45|Late Carboniferous|Carboniferous|See also Burlington granite. Of the Burlington Suite. Geological Province: Georgetown Region.||||||08-JUL-15
37808|Burlington Granite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Biotite granite, some microgranite.||||||
37808|Burlington Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Coarse-grained biotite granite; some microgranite (possibly a composite unit); hydrothermally altered biotite granite.|
37808|Burlington Granite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Coarse-grained biotite granite; some microgranite; possibly a composite unit.|
37808|Burlington Granite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.|||I-type.|
37878|Burlington Suite|23291|5|Briefly described|p96 Tb. 3.11, p100 Tb. 3.12|Late Carboniferous|Late Carboniferous|Of the O'Brien's Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27123|Burngrove Formation|13516|5|Briefly described|p145 fig 3|Late Permian|Late Permian|From Comet Ridge, Bowen Basin. Age: APP5005 - APP5006.||||||10-SEP-18
27123|Burngrove Formation|22978|6|Mentioned|p148 Fig.1|||||||||
27123|Burngrove Formation|22985|5|Briefly described|p285|Late Permian|Late Permian|||||||
27123|Burngrove Formation|22990|5|Briefly described|p315 Table 1|Late Permian|Late Permian|||||||
27123|Burngrove Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
27123|Burngrove Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
27123|Burngrove Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Blackwater Group.  Age: >251Ma.  Geological Province: Bowen Basin.||||||
27123|Burngrove Formation|29409|6|Mentioned|Table 1|||Lower part equated with Black Alley Shale||||||
27123|Burngrove Formation|29412|6|Mentioned|p209|||Also Fig.2.||||||
27123|Burngrove Formation|29724|6|Mentioned|p316|||||||||
27123|Burngrove Formation|30430|6|Mentioned|p114|||||||||
27123|Burngrove Formation|30451|6|Mentioned|p62|||||||||
27123|Burngrove Formation|30508|6|Mentioned|p85|||Three seams of non-coking coal||||||
27123|Burngrove Formation|30850|6|Mentioned|p343|||||||||
27123|Burngrove Formation|30851|6|Mentioned|p366.|||||||||
27123|Burngrove Formation|30852|6|Mentioned|Fig.2|||||||||
27123|Burngrove Formation|31079|6|Mentioned|p5|||||||||
27123|Burngrove Formation|31084|6|Mentioned|p12|||See also p26, P1.8 U. Permian. Part Blackwater Gp.||||||10-SEP-18
27123|Burngrove Formation|31531|5|Briefly described|p13|||U.Permian. See also Table 1.||||||
27123|Burngrove Formation|31620|6|Mentioned|p91|||||||||
27123|Burngrove Formation|31656|4|Described|Table 1|||U.Permian||||||
27123|Burngrove Formation|31690|6|Mentioned|p36|||||||||
27123|Burngrove Formation|31691|6|Mentioned|p427|||||||||
27123|Burngrove Formation|32177|6|Mentioned|p146|||||||||
27123|Burngrove Formation|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
27123|Burngrove Formation|32577|4|Described|p25|||U.Perm. See also p24,28-30.||||||10-SEP-18
27123|Burngrove Formation|32689|6|Mentioned|Fig.2|||Correlation table||||||
27123|Burngrove Formation|33250|5|Briefly described|p140|||||||||
27123|Burngrove Formation|33251|6|Mentioned|p2|||||||||
27123|Burngrove Formation|33390|4|Described|p5|||||||||
27123|Burngrove Formation|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
27123|Burngrove Formation|34235|6|Mentioned|p92|||||||||
27123|Burngrove Formation|34276|6|Mentioned|p42|||Permian||||||
27123|Burngrove Formation|34408|6|Mentioned|p185|||On Table||||||
27123|Burngrove Formation|35138|6|Mentioned|p16|||||||||
27123|Burngrove Formation|35433|4|Described|p27|||||||||
27123|Burngrove Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin.||||||10-SEP-18
27123|Burngrove Formation|35822|6|Mentioned|p40|||||||||
27123|Burngrove Formation|36172|6|Mentioned|Appendix|||||||||
27123|Burngrove Formation|37065|5|Briefly described|p32|||||||||
27123|Burngrove Formation|37070|6|Mentioned|p73|||||||||
27123|Burngrove Formation|37072|5|Briefly described|p90|||||||||
27123|Burngrove Formation|37073|6|Mentioned|p99|||||||||
27123|Burngrove Formation|37075|6|Mentioned|p110|||||||||
27123|Burngrove Formation|37076|4|Described|p120|||||||||
27123|Burngrove Formation|37077|6|Mentioned|p131|||||||||
27123|Burngrove Formation|37078|6|Mentioned|Fig.1|||||||||
27123|Burngrove Formation|37080|5|Briefly described|p149|||||||||
27123|Burngrove Formation|37612|6|Mentioned|Fig.3|||See also p284.||||||10-SEP-18
27123|Burngrove Formation|37726|6|Mentioned|Fig.2|||||||||
27123|Burngrove Formation|37804|6|Mentioned|p63|||||||||
27123|Burngrove Formation|38373|6|Mentioned|p613|||||||||
27123|Burngrove Formation|38518|6|Mentioned|Fig.3|||||||||
27123|Burngrove Formation|38737|6|Mentioned|p157|||||||||
27123|Burngrove Formation|38958|5|Briefly described|p493|||||||||
27123|Burngrove Formation|39212|5|Briefly described|p12|||See p13.||||||10-SEP-18
27123|Burngrove Formation|39261|6|Mentioned|Fig.6|||||||||
27123|Burngrove Formation|39267|6|Mentioned|p240|||||||||
27123|Burngrove Formation|39268|6|Mentioned|p270|||||||||
27123|Burngrove Formation|39272|5|Briefly described|p295|||Correlation||||||
27123|Burngrove Formation|39273|6|Mentioned|Fig. 2|||||||||
27123|Burngrove Formation|39445|5|Briefly described|Table 8|||See also Table 9.||||||10-SEP-18
27123|Burngrove Formation|40321|6|Mentioned|p17|||||||||
27123|Burngrove Formation|40539|6|Mentioned|Fig.2|||||||||
27123|Burngrove Formation|41191|6|Mentioned|Fig.3|||||||||
27123|Burngrove Formation|41246|6|Mentioned|Map legend|Permian||||||||
27123|Burngrove Formation|42091|6|Mentioned|p284|||||||||
27123|Burngrove Formation|42250|6|Mentioned|Fig.4 P31|||||||||
27123|Burngrove Formation|42251|6|Mentioned|Fig.2 P38|||||||||
27123|Burngrove Formation|42252|6|Mentioned|p47|||||||||
27123|Burngrove Formation|42255|6|Mentioned|p234|||||||||
27123|Burngrove Formation|42256|6|Mentioned|Fig.1 P243|||||||||
27123|Burngrove Formation|42641|6|Mentioned|p112|||||||||
27123|Burngrove Formation|42662|6|Mentioned|p84 Fig.4|||||||||
27123|Burngrove Formation|42932|5|Briefly described|p4|||||||||
27123|Burngrove Formation|43994|14|Not recorded|Map Legend||Late Permian|Part of the Blackwater Group.||||||
27123|Burngrove Formation|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
27123|Burngrove Formation|44618|14|Not recorded|p511||Permian|Ref. to Malone et al.1965.||||||10-SEP-18
27123|Burngrove Formation|44630|14|Not recorded|p494,497|||Part of Blackwater Group.||||||
27123|Burngrove Formation|45071|3|Fully described|Table 12|||||||||
27123|Burngrove Formation|45095|3|Fully described|p9|||||||||29-SEP-04
27123|Burngrove Formation|48898|2|Defined|p52|Late Permian|Late Permian|See also pp43,44,51 etc.||||||25-SEP-08
27123|Burngrove Formation|48947|5|Briefly described|p8|||||||||
27123|Burngrove Formation|49644|5|Briefly described|Table|||||||||
27123|Burngrove Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
27123|Burngrove Formation|62921|6|Mentioned|p883|||Bowen Basin. ||||Is overlain by Rangol Coal Measures. Equivalent to Betts Creek Beds (N Galilee Basin).||
27123|Burngrove Formation|67402|6|Mentioned|p21, p45, p85 tbl BWN2, p165 tbl LPB1|Capitanian|Capitanian|Bowen Basin. ||||Overlies the German Creek Formation. Overlain by the Rangal Coal Measures.||
27123|Burngrove Formation|68679|5|Briefly described|p377, p381, p383|||Malone et al. (1969). Bowen Basin. 90m thick. Freshwater prodelta, delta deposits.||||Overlies Fairhill Formation. Is overlain by Rangal Coal Measures. Passes laterally into the Black Alley Shale.|Mudstone, siltstone, labile sandstone, coal, tuff.|
27123|Burngrove Formation|70815|6|Mentioned|p3, 6, 10|||Bowen Basin. Not currently (2016) mined. Vitrinite reflectance values mapped.||||||
27123|Burngrove Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin. CA-TIMS age of 252.69 Ma (Metcalfe etal., 2015) and 252.85, 253.41, 253.45, 253.52 and 253.57 Ma (Nicoll etal., 2015). Corresponds to APP5 zone (Lopingian).||Unit of Blackwater Group.||||
27123|Burngrove Formation|70861|4|Described|p36-45|Late Permian|Late Permian|Of Bowen Basin. Contains less frequent, but thicker tuffaceous layers than Fair Hill Formation suggesting ancreased intensity in volcanism. Represents a transition from a sluggish environment with minor splays and lakes to a more active fluvial system.||Unit of Fort Cooper Coal Measures.||Uppermost unit of Fort Cooper Coal Measures. Overlain by Rangal Coal Measures. Interfingers with and overlies the Black Alley Shale.|Coal seams interbedded with laminated carbonaceous mudstone, siltstones and sandstone bodies with a mix of coarsening, and fining upward sequences.|29-AUG-19
27123|Burngrove Formation|70940|5|Briefly described|p843-845, p848, p850-855|Permian|Permian|Northern Taroom Trough, central Bowen Basin. Decompacted thickness of 212m deposited in 0.88 Ma. Sedimentation rates discussed in some detail. Contains numerous tuff layers which can be used for correlation across the Basin.||Blackwater Group.||Overlies Fair Hill Formation and Black Alley Shale. Is overlain by Yarrabee Tuff.||
27123|Burngrove Formation|71265|5|Briefly described|p587, p589-590, p592, p598-607|Changhsingian|Changhsingian|Bowen and Galilee Basins. Represents a southerly-prograding fluvial-deltaic system during late-Lopingian regression. References to "Burngrove Formation equivalent". Previously the lower section of Bandanna Formation; reassigned by Phillips et al. (2017). Sedimentary logs of CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Overlies Black Alley Shale. Is overlain by Bandanna Formation. With Fair Hill Formation, is equivalent to Fort Cooper Coal Measures.|Fine sandstones with low-angle to horizontal bedding and lamination, with abundant sideritic horizons; numerous tuffaceous horizons. Capped locally by a tuffaceous coal seam, or anoxic dark shales interbeddeed with tuffaceous material.|
27123|Burngrove Formation|71276|5|Briefly described|p295-297|Lopingian|Lopingian|Southern Bowen Basin.||||Overlies Fair Hill Formation, and Black Alley Shale conformably. Is overlain by Bandanna Formation.|A distinct deltaic coarsening-upward sequence, punctuated by coal seams.|
27123|Burngrove Formation|71701|4|Described|p153, p155-p156, p158-p159, p168-p169|Lopingian|Lopingian|Eastern Area; Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin. An equivalent that was originally referred to as the B coal-seam is the source of the dates provided. Intersected in CRD Montani 1, OEC Glue Pot Creek 1 and GSQ 1-1A. An upper CA-IDTIMS age of 252.81 +/- 0.07 Ma is provided at the top of this unit in CRD Montani 1.||Betts Creek Group||Overlies the Black Alley Shale. Overlain by the Bandanna Formation.||
27123|Burngrove Formation|71710|6|Mentioned|p367|||Bowen Basin. Dates of Betts Creek beds equivalents correlated with radiometric ages of this formation.||||||22-MAY-19
27123|Burngrove Formation|72297|5|Briefly described|p694 Fig.10.8|Permian|Permian|Bowen Basin.||||Overlies Fair Hill Formation. Is overlain by Rangal Coal Measures. Correlated with Black Alley Shale and Kaloola Member.|Contains coal seams and tuffs.|
27123|Burngrove Formation|73163|6|Mentioned|p468|Lopingian|Lopingian|Bowen Basin.||||Overlain by Yarrabee Tuff.||
27123|Burngrove Formation|73246|6|Mentioned|p190|Upper Permian|Upper Permian|Bowen Basin, central.||Blackwater Group||Underlain by Fair Hill Formation. Overlain by Rangal Coal Measures. Equivalent to Fort Cooper Coal Measures.||
27123|Burngrove Formation|73305|4|Described|p547-548, p550-p551, p554-555, p557-p561|Late Permian|Late Permian|Northern Bowen Basin. Grades into the Black Alley Shale in the Denison Trough (Anderson, 1985). Thickness varies from 6.6 to 214.6 m, greatest at the junction of the Collinsville Shelf and Nebo Synclinorium. Thins abruptly in the Denison Trough. Merged coals in the north split and thin southwards at the boundaries of morphotectonic zones. Named coal seams include the Girrah, Lower Vermont, BG3, Lower Pisces, Virgo, Libra, Leo and Aquarius seams. See also p550 Fig.3, p553 Fig.5, p554, p555 Fig.7, p556 Tb.3, p558 Fig.10.||Fort Cooper Coal Measures|Yarrabee Tuff, Girrah Seam, Lower Vermont Seam, BG3 Seam|Overlies the Black Alley Shale, Middle Main Seams. Overlies Fair Hill and equivalent formations in southeast parts of basin. Interbedded with Kaloola Member.|Characterised by a number of traceable coal seams and tuffaceous horizons with sandstone-dominated interburden, capped by the Yarrabee Tuff.|12-FEB-23
27123|Burngrove Formation|73625|5|Briefly described|p5 Fig.3, p13, 20-21|Permian|Permian|Comet Ridge, Bowen Basin.||||Overlies Fairhill Formation. Is overlain by Rangal Coal Measures. Equivalent to Black Alley Shale.|Includes localised, plant-fossil-rich, permineralised peats associated with silica-rich ash deposits.|
23445|Burns Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23445|Burns Granite|22781|4|Described|p31|Early Devonian|Early Devonian|Ebagoola Suite||||||
23445|Burns Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite.||||||
23445|Burns Granite|42610|2|Defined|p13|Early Devonian|Early Devonian|Age assumed similar to Barwon Granite, about 400Ma. Included in "Kintore Adamellite" of B135.||||||
23445|Burns Granite|71849|5|Briefly described|p8, p14, p149, p155-156, p195|Devonian|Devonian|Included in Ebagoola Suite by Mackenzie and Knutson (1992).||Ebagoola Suite.|||White to pale grey, medium- to coarse-grained, even-grained to slightly porphyritic (garnet-)muscovite-biotite granite. High-K calc-alkaline S-type.|
23445|Burns Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.||Grades into Heneage Granite.|Pale grey to cream or brown, medium to coarse muscovite-biotite granite, sparsely porphyritic in places.|
38864|Burns Spur Nepheline Monzosyenite|24488|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.  Altered pale pink medium grained leucocratic ferrohastingsite-lepidomelane-melanite nepheline monzosyenite.||||||
38864|Burns Spur Nepheline Monzosyenite|68008|3|Fully described|p399-400, p444, p447-453|Early Cretaceous|Early Cretaceous|A small (2 x 1km) feldspathoid-bearing intrusion c.6km SW of Radley Nepheline Syenite. Named after the old Burns Spur mine. The type area is along a stream (either Ridley Creek or a tributary) flowing NE and dividing the intrusion into approximately equal parts. Forms steep dissected slopes of Dawes Range. Geophysics briefly described: contrasted with Monal Granodiorite. No geochemical analysis. Age from correlation. Hosted the old Burns Spur copper mine. Appears as Burns Spur Nepheline Monzonite on p399-400.||Glassford Igneous Complex.||Intrudes Monal Granodiorite and Ridler Monzonite. Correlated with Radley Nepheline Syenite.|Pink to fawn, medium- to coarse-grained, equigranular, leucocratic nepheline monzosyenite with local concentrations of large finer-grained grey inclusions. Sulphides (mainly pyrite) relatively abundant along irregular joint planes.|
38864|Burns Spur Nepheline Monzosyenite|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Goondicum Gabbro, Judas Trachybasalt, Radley Nepheline Syenite, Ridler Monzonite, Tollbar Breccia, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
38864|Burns Spur Nepheline Monzosyenite|69594|5|Briefly described|p560-561|Cretaceous|Cretaceous|Whitsunday Volcanic Province.||Glassford Igneous Complex.||Intrudes Monal Granodiorite and Ridler Monzonite.|Leucocratic nepheline monzosyenite, dominated by poikilitic miroperthitic K-feldspar with lesser plagioclase, nepheline, muscovite and mafic phases. Detailed on p561.|
38864|Burns Spur Nepheline Monzosyenite|73450|4|Described|p11, p63, p65-66|early Cretaceous|early Cretaceous|[Misspelt as Burns Spur Nepheline Syenite on p. 60, 62, 64]. Described by Murray et al. (2012). Forms small NE aligned, feldspathoid-bearing pluton; exposed in the steep, dissected slopes of the Dawes Range. May be related to the Radley Nepheline Syenite, Ridler Monzonite, and Judas Trachybasalt.||Glassford Igneous Complex||Intrudes Monal Granodiorite and Ridler Monzonite.|Pink to fawn, medium- to coarse-grained, leucocratic nepheline monzosyenite.|
25823|Burstall Granite|22522|6|Mentioned|p337||Statherian|Max Age: ca 1740 Ma||||||
25823|Burstall Granite|22722|6|Mentioned|p271,274|Statherian|Statherian|||||||
25823|Burstall Granite|22723|6|Mentioned|p262,3|Statherian|Statherian|Sometimes refered to in text as Informal Burstall granite, lower case g also used on figure 3 p263.||||||21-OCT-19
25823|Burstall Granite|23071|5|Briefly described|p760|Statherian|Statherian|||||||
25823|Burstall Granite|23324|4|Described|p467, p468 Fig. 1|||Metagranite and acid dykes. Age: 1740-1700Ma.||||||07-FEB-07
25823|Burstall Granite|23959|6|Mentioned|p1166|||Intrudes the Corella Formation.  Geological Province: Mount Isa Inlier.||||||
25823|Burstall Granite|24197|5|Briefly described|p32, p94 Tb. 1.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
25823|Burstall Granite|24253|6|Mentioned|p6|||Geological Province: Mount Isa Block.||||||
25823|Burstall Granite|24255|5|Briefly described|p33 Fig.2|Statherian|Statherian|Geological Province: Eastern Succession, Mount Isa Block. Age: 1740-1735 Ma.||||||
25823|Burstall Granite|24257|5|Briefly described|p67|Paleoproterozoic|Paleoproterozoic|Age: 1740-1735 Ma. Geological Province: Eastern fold belt, Mount Isa Block.||||||07-NOV-08
25823|Burstall Granite|24259|6|Mentioned|p107 Fig.1|||Geological Province: Mount Isa Block.||||||
25823|Burstall Granite|29550|5|Briefly described|p44|||||||||
25823|Burstall Granite|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25823|Burstall Granite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
25823|Burstall Granite|30531|6|Mentioned|p20|||Also mention p22.||||||21-OCT-19
25823|Burstall Granite|30536|6|Mentioned|Fig.3|||||||||
25823|Burstall Granite|30601|6|Mentioned|p419|||||||||
25823|Burstall Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25823|Burstall Granite|32660|5|Briefly described|Table 5|||||||||
25823|Burstall Granite|32959|6|Mentioned|p31|||||||||
25823|Burstall Granite|33900|5|Briefly described|p23|||See also p15.||||||21-OCT-19
25823|Burstall Granite|35000|6|Mentioned|p137|||||||||
25823|Burstall Granite|35074|6|Mentioned|Fig.2|||||||||
25823|Burstall Granite|35167|2|Defined|p153|Late Precambrian|Late Precambrian|||||||
25823|Burstall Granite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
25823|Burstall Granite|35495|6|Mentioned|p344|||||||||
25823|Burstall Granite|35932|6|Mentioned|p457|||||||||
25823|Burstall Granite|36052|6|Mentioned|Fig.1|||See also Fig.2.||||||
25823|Burstall Granite|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
25823|Burstall Granite|37462|4|Described|Table4.VII|||||||||
25823|Burstall Granite|37568|6|Mentioned|p85|||||||||
25823|Burstall Granite|37569|6|Mentioned|p92|||||||||
25823|Burstall Granite|37862|6|Mentioned|p586|||||||||
25823|Burstall Granite|38235|6|Mentioned|p115|||||||||
25823|Burstall Granite|38238|6|Mentioned|p135|||||||||
25823|Burstall Granite|38276|6|Mentioned|Fig.1|||||||||
25823|Burstall Granite|38350|6|Mentioned|p18|||||||||
25823|Burstall Granite|38560|6|Mentioned|p115|||||||||
25823|Burstall Granite|38833|6|Mentioned|p161|||||||||
25823|Burstall Granite|38834|6|Mentioned|p162|||||||||
25823|Burstall Granite|39049|4|Described|p840|||||||||
25823|Burstall Granite|39445|6|Mentioned|p43|||1740 Ma. See also Table 2||||||
25823|Burstall Granite|39492|6|Mentioned|p30|||||||||
25823|Burstall Granite|39622|6|Mentioned|p28|||||||||
25823|Burstall Granite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25823|Burstall Granite|39937|6|Mentioned|p79|||||||||
25823|Burstall Granite|39998|6|Mentioned|p191|||||||||
25823|Burstall Granite|40840|6|Mentioned|Map legend|||||||||
25823|Burstall Granite|41125|6|Mentioned|p45|||||||||
25823|Burstall Granite|41150|5|Briefly described|p1806|||||||||
25823|Burstall Granite|41465|5|Briefly described|p11|||||||||
25823|Burstall Granite|41791|6|Mentioned|p270|||||||||
25823|Burstall Granite|41979|6|Mentioned|p525|||||||||
25823|Burstall Granite|42201|6|Mentioned|p294|||||||||
25823|Burstall Granite|42365|5|Briefly described|Fig.1 P256|||Also Fig.3, Fig.15.||||||21-OCT-19
25823|Burstall Granite|42438|5|Briefly described|p275|||||||||
25823|Burstall Granite|42565|6|Mentioned|p7|||||||||
25823|Burstall Granite|42781|5|Briefly described|Fig.4 P429|||See also Fig.1 p426.||||||21-OCT-19
25823|Burstall Granite|42879|6|Mentioned|p214|||||||||
25823|Burstall Granite|43595|5|Briefly described|p437||Mesoproterozoic|U-Pb dating: 1740-1730 Ma.||||||21-OCT-19
25823|Burstall Granite|43615|6|Mentioned|p14|||1740 Ma||||||
25823|Burstall Granite|43616|6|Mentioned|p4|||Age 1730-1740 Ma||||||
25823|Burstall Granite|45136|3|Fully described|p24|||Also described p60.||||||06-FEB-07
25823|Burstall Granite|45161|6|Mentioned|p32|||||||||
25823|Burstall Granite|45166|5|Briefly described|p20|||||||||
25823|Burstall Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25823|Burstall Granite|46843|6|Mentioned|Fig.2|||||||||
25823|Burstall Granite|46960|6|Mentioned|p217|||||||||
25823|Burstall Granite|46976|6|Mentioned|Fig.1|||||||||
25823|Burstall Granite|46996|6|Mentioned|p273|||||||||
25823|Burstall Granite|49009|6|Mentioned|p38|||||||||
25823|Burstall Granite|49041|5|Briefly described|Table 2|||||||||
25823|Burstall Granite|50100|5|Briefly described|p13 Fig.4, p18|Statherian|Statherian|Of the Burstall Suite of the Wonga Batholith.  Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||06-FEB-07
25823|Burstall Granite|50332|5|Briefly described|p19, p77|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1760-1720Ma. Intruded into the Kalkadoon-Ewen Province and Eastern Fod Belt Province. Geological Province: Kalkadoon-Ewen Province and Eastern Fod Belt Province.||||||07-FEB-11
25823|Burstall Granite|50536|5|Briefly described|p1.4, 6.1 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite. Age: 1745-1726 +/- 16Ma (U-Pb).||||||07-NOV-08
25823|Burstall Granite|63866|5|Briefly described|p60-p61|||Wonga Belt.||Burstall Suite||||
25823|Burstall Granite|65396|6|Mentioned|p6, p75, p85-86, p90, p386|||Associated with Mary Kathleen U-REE orebody.|~1740 Ma|||||
25823|Burstall Granite|65505|5|Briefly described|976, 980, Fig 1-3,7|Proterozoic|Proterozoic|Of the Burstall Suite. Felsic. Pink, massive, weakly foliated, coarse-grained, with K-feldspar phenocrysts. Age: 1737 +/- 3 Ma.||||||
25823|Burstall Granite|66529|5|Briefly described|p61-62, p64, p82, p93    |||Associated with garnet-pyroxene skarn of Mary Kathleen U-REE deposit.|1740 -1730 Ma (Page, 1983).|||Intrudes the Corella Formation.||
25823|Burstall Granite|67127|6|Mentioned|p96|||Fluids associated with this unit could have leached REE from the Corella Formation to form a REE-rich skarn protore. Interpreted to be related to the formation of skarns.|~1740 Ma (U-Pb TIMS)|||||
25823|Burstall Granite|67323|4|Described|p18; GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier. Wonga/Burstall Igneous Event.|1740 +/- 3 Ma.|Wonga Suite, Burstall Suite.||Intrudes Corella Formation.|Pink, foliated, medium to coarse-grained, leucocratic biotite granite|
25823|Burstall Granite|67497|6|Mentioned|p911 Fig.20|Statherian|Statherian|Age from Nd isotope evolution diagram (p911 Fig.20).|c.1745 - c.1720 Ma|||||23-APR-13
25823|Burstall Granite|67539|6|Mentioned|p7|||Occur as intrusions throughout the Corella Formation belt.||||||
25823|Burstall Granite|68020|6|Mentioned|p127|||Has elevated U content.|1737 +/- 15 Ma|||||
25823|Burstall Granite|68021|6|Mentioned|p135 fig 4, p136|Statherian|Statherian|Spelt Burstal Granite fig.4.|1740 Ma|||Intrudes Corella Formation and possibly Marraba Volcanics, Mitakoodi Quartzite, Ballara Quartzite.||
25823|Burstall Granite|68542|6|Mentioned|p20 fig 6, p21||||1740 Ma|||||
25823|Burstall Granite|68576|6|Mentioned|Q_2: p20-21|||Mary Kathleen area.|1740 Ma.|||||
25823|Burstall Granite|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|Igneous crystallisation ages.|1737 +/- 3, 1740 +/- 3 Ma|||||
25823|Burstall Granite|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1737 +/- 3 Ma.|||||
25823|Burstall Granite|69591|5|Briefly described|p60||||1740 +/- 3 Ma (Neumann et al., 2009).|Burstall Suite.|||Pink, foliated medium- to coarse-grained leucocratic biotite granite.|
25823|Burstall Granite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink, foliated, medium- to coarse-grained, leucocratic biotite granite. Separately mapped are tourmaline pegmatite; pegmatite, locally garnetiferous; microgranite dykes; microgranite with garnet, diopside and albite; leucocratic metagranite.|
25823|Burstall Granite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink, foliated, medium- to coarse-grained, leucocratic biotite granite. Separately mapped are tourmaline pegmatite; pegmatite, locally garnetiferous; microgranite dykes; microgranite with garnet, diopside and albite; leucocratic metagranite.|
25823|Burstall Granite|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.|1740 Ma.|||||
25823|Burstall Granite|71592|5|Briefly described|Appendix A.|||Mary Kathleen Domain, Mount Isa Orogen.|1737+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite, gneiss, rhyolite.|
25823|Burstall Granite|72596|6|Mentioned|p1-2, p9, p40, p46|Statherian|Statherian|Geochronologic constraint from Neumann et al. (2009). Correlated with / compositionally similar to the granitic component of the Mount Erle Complex and Myubee Igneous Complex, and the Overlander and Revenue granites (see Bultitude et al., 1982; Blake et al., 1984).|1740 +/- 3 Ma, 1737 +/- 3 Ma, SHRIMP U-Pb|Burstall Suite||Coeval with metarhyolite of the Corella Formation, elsewhere intrudes the Corella Formation [?].||
25823|Burstall Granite|72799|4|Described|p1, p3, p5, p10, p19, p38, p46-50, p56|Statherian|Statherian|Geochron is a new magmatic crystallisation age of subunit 1. This subunit is a leucocratic metagranite that forms a small body at the northeastern tip of the unit, ca 5 km northwest of the Mary Kathleen Mine. It is more leucocratic, apparently unfoliated, and shows indicators of high-level emplacement compared to the main body of the unit. New age is within error of previous ages for the unit, which demonstrates the subunit is co-magmatic with the main unit. Geochronology in the report also indicates the unit is contemporaneous with an unnamed miarolitic leucogranite at Mount Colin, and may be associated despite differences in mineralogy, texture and degree of foliation.|1736 +/- 4 Ma SHRIMP U-Pb|Burstall Suite||Intrudes Corella Formation. Coeval with Lunch Creek Gabbro, Myubee Igneous Complex, and Wimberu Granite.|Includes miarolitic biotite granite.|
25823|Burstall Granite|73413|6|Mentioned|p6, App.1|Statherian|Statherian|U-Pb TIMS ages of 1745 +/- 16 Ma, 1737+/- 15 Ma, and 1726 +/- 8 Ma reported by Page (1983). U-Pb SHRIMP age of 1740 +/- 3 Ma and 1737 +/- 3 Ma reported by Neumann et al. (2009).|ca. 1726-1745 Ma|||||
25823|Burstall Granite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Kalkadoon-Leichhardt and Mary Kathleen Domain.|1737+/-3 Ma crystallisation age||||Felsic intrusive.|
25823|Burstall Granite|73529|6|Mentioned|p2 Fig.1, p14|||Sill-like magmatic body, folded during Isan Orogeny.||Burstall Suite||||
25823|Burstall Granite|73553|4|Described|pp3, p8, p18, p32, p36, p44, p79-81,|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Initially included in the Wonga Granite (Carter et al., 1961). Most intrusions included as the Burstall Granite defined by Derrick et al., (1978) are now mapped as individual units. Burstall Granite is now restricted to the main body east and northeast of Mary Kathleen. Elongate pluton up to 5 km wide. Low to moderate magnetic response, bright white to slightly pinkish tones on radiometric images. Close spatial association and complex contact with Lunch Creek Gabbro, suggested that the granite intrudes the gabbro. Coeval with Wonga Granite. Gogenetic with Mount Godkin Granite. Multiple ages provided, most recent SHRIMP zircon U-Pb ages range from 1740+/-3 Ma to 1736+/-4 Ma. See also p100-101, p117-118, p122, p126-127, p131-132, p135-146, p153, p165, p173, p176, p185, p187, p216, p221, p224, p226, p247, p249, p258, p266.|1726+/-8 Ma (TIMS), 1745+/-16 Ma U-Pb zircon|Burstall Suite||Intrudes Corella Formation, intruded by Lakeview Dolerite|Pink, foliated, medium- to coarse-grained, leucocratic biotite granite; pegmatite, locally garnetiferous; microgranite dykes; leucocratic metagranite; tourmaline pegmatite.|03-FEB-23
24799|Burstall Suite|23545|5|Briefly described|p605.|||||||||
24799|Burstall Suite|24197|5|Briefly described|p28, p32, p92|Paleoproterozoic|Paleoproterozoic|Example of the Hiltaba Association. Comprises Mount Godkin, Burstall, Overlander, Revenue and Saint Mungo Granites, Mount Earle Igneous Complex and possibly the Myubee Igneous Complex also. Age:~1740Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
24799|Burstall Suite|42201|5|Briefly described|p292|||||||||
24799|Burstall Suite|42781|6|Mentioned|Fig.12 P442|||||||||
24799|Burstall Suite|50100|5|Briefly described|p11, p18|Proterozoic|Proterozoic|Includes the Burstall, Overlander, Revenue and Saint Mungo Granites and the Mount Erle and Myubee Igneous Complexes. Intrudes the Corella Formation. Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||13-OCT-08
24799|Burstall Suite|50332|6|Mentioned|p16, p19|Proterozoic|Proterozoic|Includes; Burstall Granite and Mount Godkin Granite, Lunch Creek Gabbro. Characterised by common association with coeval gabbros.||||||07-FEB-11
24799|Burstall Suite|50536|5|Briefly described|p1.1, 1.4, 6.1 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1740Ma.||||||07-NOV-08
24799|Burstall Suite|63023|6|Mentioned|p1024 Fig. 1|||||||||
24799|Burstall Suite|63866|5|Briefly described|p61||||||Includes the Burstall Granite.|||
24799|Burstall Suite|65387|5|Briefly described|p84|Statherian|Statherian|Probable source of younger detrital zircons in Knapdale Quartzite and Quamby Conglomerate.|c.1760-1730 Ma (Neumann, 2007).|||||
24799|Burstall Suite|65455|6|Mentioned|p7, p8 Fig. 4|||Mount Isa region, central belt. Granitoids show patchy enrichment.||||||09-MAY-12
24799|Burstall Suite|65505|6|Mentioned|966, 976, 980|Proterozoic|Proterozoic|Flanks the Wonga Batholith. North-trending granite in Mary Kathleen Fold Belt. Age: 1745+/-6 Ma.||||||
24799|Burstall Suite|67127|6|Mentioned|p94|||Deposited during the Wonga Extension Event.|ca. 1760 -1720 Ma|||||
24799|Burstall Suite|67323|4|Described|p15, p24, p31, p107; Solid Geology Map|||See also Wonga Suite, Burstall Suite. Mary Kathleen Domain. Intruded shear zone and upper plate at ~1740 Ma. Two other, similar, ages are given.|1739 +/- 3 Ma.||Lunch Creek Gabbro.|Time-equivalent to the Wonga Suite.|Bimodal intrusives.|
24799|Burstall Suite|67497|5|Briefly described|p909||||||Includes Mount Erle Igneous Complex, Revenue Granite.|||
24799|Burstall Suite|68146|5|Briefly described|p1, p194|||Mary Kathleen Belt. This age coincides with the 1760-1740 ma Inkamulla Igneous Event in the NT.|c.1740-1735 Ma.|||||
24799|Burstall Suite|68542|6|Mentioned|p1, p15|||||||||
24799|Burstall Suite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, the Wonga Suite and Gin Creek Granite are all mapped under the same symbol, -Pgw.||||||
24799|Burstall Suite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
24799|Burstall Suite|69056|4|Described|p2-3, p5, p53, Reference images sheet|Statherian|Statherian|Shown on the simplified surface and solid geology maps of the Quamby Project area. Intrudes the Mary Kathleen and Constantine Domains. Also appears as Wonga-Burstall Suite on p4-5. Associated with the ~1740 Ma Wonga Event. Coeval with Wonga Suite.|~1740 Ma.||Mount Godkin Granite.|Intrudes Argylla and Corella Formations.|Bimodal, largely unfoliated intrusives.|
24799|Burstall Suite|69591|5|Briefly described|p28, p36, p60|Paleoproterozoic|Paleoproterozoic|Mary Kathleen Domain, Mount Isa Province. Emplacement correlates with the ~1740 Ma Wonga Extension Event which affected the Double Crossing Metamorphics and produced the Gin Creek Granite.|||Burstall, Houdini, Mount Godkin, Overlander, Revenue, Saint Mungo Granites; Lunch Creek Gabbro; Mount Erle Igneous Complex; Mount Philp Breccia.||Deformed granite.|
24799|Burstall Suite|72596|6|Mentioned|p1, p4, p40|Statherian|Statherian|Distribution shown in Fig i.|~1740 to 1718 Ma||Burstall Granite, Mount Erle Igneous Complex, Revenue Granite, Overlander Granite, Myubee Igneous Complex.|||
24799|Burstall Suite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|||Includes Mount Earle Igneous Complex, Mount Philp Breccia, Overlander Granite, Revenue Granite|Shown as older than Lakeview Dolerite. Equivalent age to Wonga Suite .||
24799|Burstall Suite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coeval with the Wonga-Burstall Event (c. 1740 Ma).|||Includes Mount Earle Igneous Complex, Mount Philp Breccia, Overlander Granite, Revenue Granite|Shown as older than Lakeview Dolerite. Equivalent age to Wonga Suite .||
24799|Burstall Suite|72799|6|Mentioned|p1, p4-5, p38|Statherian|Statherian||ca. 1740 Ma||Mount Godkin Granite, Burstall Granite, Lunch Creek Gabbro[?]|||
24799|Burstall Suite|72889|6|Mentioned|p6 Fig.i., p28|||||||||25-NOV-20
24799|Burstall Suite|73413|6|Mentioned|p2-3, p5-6, p20-22, App.1|Statherian|Statherian|Mary Kathleen Domain. [Age written as 1740-1730 Ma, 1780-1720 Ma, 1745-1730 Ma, and 1740 Ma]. Intrude rocks of Cover Sequence 2 (of Foster and Austin, 2008).|1780-1720 Ma||Saint Mungo Granite||May include granites and gabbros.|
24799|Burstall Suite|73529|5|Briefly described|p1, p2 Fig.1, p4, p14, p15 Fig.11|Statherian|Statherian|Mary Kathleen Domain, intrudes sedimentary succession. Located in low strain domains. Emplacement ages mostly overlap with Wonga Suite.|1750-1710 Ma||Myubee Granite, Revenue Granite, Overlander Granite, Burstall Granite, Mount Godkin Granite, Myubee Gabbro|Intrudes Corella Formation|Multi-phase plutons, typically weakly deformed to undeformed.|
24799|Burstall Suite|73553|5|Briefly described|p1, p108, p132, p142, p144,|||Formerly included Saint Mungo Granite. See also Burstall suite p142. See also 'Wonga Suite, Burstall Suite' p54 [from GIS geological compilation]. Mount Philp Breccia included by Hutton and Withnall, (2013), argued that there is little justification for this based on composition and age. See also p144, p244, p146, p156, p166, p223.|||Overlander Granite, Mount Godkin Granite, Burstall Granite, Lunch Creek Gabbro, Revenue Granite, Mount Erle Igneous Complex, Myubee Igneous Complex, Mount Philp Breccia|||03-FEB-23
27998|Burton Lagoon Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes the Yambo Metamorphic Group||||||
27998|Burton Lagoon Granite|43596|4|Described|p35, p26 Tb. 2, p27 Tb. 3|||Of Ebagoola Suite (Kintore Supersuite). Intrudes Oswald and Annie Creek Schists.||||||15-JAN-09
27998|Burton Lagoon Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
35093|Burwood Complex|23042|4|Described|p17,8,21,3,30,71-3, Fig 2|Carboniferous|Carboniferous|Intrudes Cycle 2 of Connors Volcanics.||||||
35093|Burwood Complex|60475|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Bioitte hornblende granodiorite, quartz monzonite, quartz monzodiorite and diorite; some leucogranite and hornblende biotite monzogranite.||||||
35093|Burwood Complex|60480|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Biotite hornblende granodiorite, quartz monzonite, quartz monzodiorite and diorite; some leucogranite and hornblende biotite monzogranite.||||||
35093|Burwood Complex|61035|4|Described|p6, p10 Tb. 1|Early Carboniferous|Early Carboniferous|Intrudes Mountain View Volcanics and unconformably overlain by Leura Volcanics. Age: 332+/-3Ma (M. Fanning, SHRIMP). Geological Province: Connors Sudprovince. For lithology see p10 Tb. 1.||||||07-FEB-11
35093|Burwood Complex|65388|2|Defined|p351-352, p86, p90, 94, 98, 100, 106|Early Carboniferous|Early Carboniferous|Connors Arch composite pluton. Three unnamed components delineated. SHRIMP age 328 +/-4 Ma. K-Ar ages have been partially reset. Intrudes and has hornfelsed Mountain View Volcanics. Unconformably overlain by  Leura Volcanics and breccia clasts in Lotus Creek Rhyolite indicate that it postdates Burwood Complex. Includes grey to pinkish grey, medium-grained, equigranular biotite-hornblende granodiorite to quartz monzodiorite. See also p354, 393, 399, 447.||||||
35093|Burwood Complex|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
35093|Burwood Complex|68679|5|Briefly described|p347, p353, p355-357, p363|Mississippian|Mississippian|Northern New England Orogen.|328.0 +/- 3.8 Ma (SHRIMP: Fanning et al., 2009).|||Intrudes the Mountain View Volcanics. Is overlain unconformably by Leura Volcanics.||
35093|Burwood Complex|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|328+/-3.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
74879|Bushley Dacite|68008|2|Defined|p223-225, p233, p248|Early Jurassic|Late Triassic|Defined in this study. Bushley-Wycarbah district. Named after locality and siding at Bushley. The type area is along the main central railway from Bushley to the railway crossing 2km further west; exposed in cuttings. Forms low, dissected ridges. Over 100m thick. Geochemistry detailed; it is the oldest unit in the Yarrol Project area with unequivocal within-plate geochemical signature. Appears as Bushley Volcanics on p233.||||Overlies Umbrella Granodiorite nonconformably. Is overlain by Precipice Sandstone, probably unconformably, and Dalma Basalt.|Mainly dacite to trachyte or trachyandesite flows, purple to black and typically flow-banded.|
74879|Bushley Dacite|69594|6|Mentioned|p551 Fig.7.22|Jurassic|Triassic|||||||
74879|Bushley Dacite|73450|4|Described|p51-52, p54|Jurassic|Triassic|Defined by Murray et al. (2012). Restricted spatial extent forming a belt of low hills between Bushley and Wycarbah.||||Overlain by Precipice Sandstone.|Flow-banded dacite to trachyte or trachyandesite flows.|
24204|Bushy Park Gneiss|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24204|Bushy Park Gneiss|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24204|Bushy Park Gneiss|37862|4|Described|p585|||||||||
24204|Bushy Park Gneiss|38350|4|Described|p17|||||||||
24204|Bushy Park Gneiss|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24204|Bushy Park Gneiss|38658|6|Mentioned|p152|||||||||
24204|Bushy Park Gneiss|39445|6|Mentioned|Table 2|||||||||
24204|Bushy Park Gneiss|40840|6|Mentioned|Map legend|||||||||
24204|Bushy Park Gneiss|45161|5|Briefly described|p31|||See also p19 and Fig.8||||||11-OCT-22
24204|Bushy Park Gneiss|45166|5|Briefly described|p34|||||||||
24204|Bushy Park Gneiss|49009|2|Defined|p9|Proterozoic|Proterozoic|Mapped as Argylla Fm,Corella Fm. & Kalkadoon Gr. (Carter & Opik,1963).||||||18-AUG-08
24204|Bushy Park Gneiss|49041|5|Briefly described|Table 2|||||||||
24204|Bushy Park Gneiss|50100|5|Briefly described|p18, p78|Proterozoic|Proterozoic|Of the Wonga Suite (Wonga Batholith). Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||18-AUG-08
24204|Bushy Park Gneiss|50536|5|Briefly described|p1.4, 5.2 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.||||||07-NOV-08
24204|Bushy Park Gneiss|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzofeldspathic gneiss, augen gneiss, gneissic granite.||||||
24204|Bushy Park Gneiss|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Felsic hornblende-biotite gneiss, augen gneiss.|
24204|Bushy Park Gneiss|69591|5|Briefly described|p60|||Wonga Batholith.|||||Felsic hornblende-biotite gneiss, augen gneiss.|
24204|Bushy Park Gneiss|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Felsic hornblende-biotite gneiss, augen gneiss.|
24204|Bushy Park Gneiss|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Felsic hornblende-biotite gneiss, augen gneiss.|
24204|Bushy Park Gneiss|73137|4|Described|p1, p5, p95-96, p98-101|Orosirian|Orosirian|Mary Kathleen Domain, western. Crops out in a narrow, northerly trending zone of intense deformation. Previously interpreted to post-date the Magna Lynn Metabasalt and Argylla Formation, and was previously tentatively correlated with the Wonga Granite (thus, emplaced at ~1740 Ma) [however, the new geochron does not support the previous interpretations]. Geochron is magmatic crystallisation age, which is similar to Kalkadoon-Leichhardt Domain basement units. Indicates that the high-strain zone forming the western part of the Mary Kathleen Domain contains lenses of older, basement rocks that have been tectonically interleaved with younger units.|1860 +/- 5 Ma||||Granitic gneiss and gneissic granitoid, including dark grey, fine-grained gneissic granodiorite, interlayered with other units.|
24204|Bushy Park Gneiss|73529|6|Mentioned|p6 Fig.3, p8, p14||||||||Intrusive unit.|
24204|Bushy Park Gneiss|73553|5|Briefly described|p1, p6, p13-19, p37, p43-45, p47,|Orosirian|Orosirian|Included in Kalkadoon-Leichhardt Igneous Province based on geochronology. Located in a narrow northerly trending high-strain zone on the W margin of the Mary Kathleen Domain, forms scattered elongate lenses and pods. Interlayered with rocks mapped as Magna Lynn Metabasalt, Argylla Formation, Corella Formation. Previously, tentatively correlated with similar rocks to the north and assigned to Wonga Suite by Budd et al., (2001). Type area at MGA 375046 7646244, ~11 km NW of Duchess. Largest outcrops show distinct geophysical characteristics of pale green tones on radiometric images, low response on aeromagnetic images. A-type. Approximate U-Pb zircon LA-ICP-MS age of >1900 Ma (unpublished). See also Busy Park Gneiss p8 Fig.1.2.3. See also p53-54, p59, p80-81, p157-158, p224, p228, p230, p246-247, p249-p250.|1860+/-4 Ma (Kositcin et al., 2021)||||Pinkish grey, fine- to medium-grained gneissic granite with numerous pale pink microcline megacrysts; dark grey biotite-rich gneissic granodiorite. Strongly deformed and almost completely recrystallised.|03-FEB-23
41293|Bustard Head Granodiorite|60015|4|Described|p81-83|Triassic|Triassic|Type locality described.  Pink alkali-feldspar and plagioclase, transparent grey quartz, cream to pale green altered plagioclase, chloritised hornblende and minor black flakes of chloritised biotite.||||||13-JUN-13
41293|Bustard Head Granodiorite|65452|6|Mentioned|p6 Fig.2, p29|Late Triassic|Late Triassic|Appears as Bustard head Granodiorite in Fig.2. Geochemistry briefly described.||||||
41293|Bustard Head Granodiorite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink medium-grained, uneven-grained to porphyritic, leucocratic biotite monzogranite; locally granophyric, miarolitic to gabbro enclaves (net-veined complex?).|
41293|Bustard Head Granodiorite|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|von Gnielinski et al. (2004).|||||Pink, medium-grained, equigranular biotite granodiorite to syenogranite. Large areas of abundant microdiorite to gabbro enclaves (net-vein complex?).|
80559|Buthen Buthen Suite|71792|5|Briefly described|p26|Devonian|Late Silurian|Newly delineated, as a result of recent investigations. Age inferred.||Kintore Supersuite|Includes the Buthen Buthen Granite.|||09-AUG-18
80559|Buthen Buthen Suite|71849|4|Described|p2-3, p8, p13, p50, p111, p147-148|Devonian|Devonian|See also p150-154, p159, p161-162, p176, p195. Coen Inlier. Recognition of this unit is based on very few analyses. Also includes an unnamed unit in the Wenlock area. Geochemistry described.||Kintore Supersuite.|Buthen Buthen Granite and Whites Creek Granodiorite.||Calc-alkaline to high K calc-alkaline.|
80559|Buthen Buthen Suite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|Buthen Buthen Granite.|||
80559|Buthen Buthen Suite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|Buthen Buthen Granite, Whites Creek Granodiorite.|||
27355|Butlers Volcanic Group|23032|4|Described|p42||Carboniferous|||||||
27355|Butlers Volcanic Group|23291|4|Described|p42, p91 Tb. 3.9|Carboniferous|Carboniferous|Intruded by Sues Creek Microgranite and Noel Micromonzonite. Geological Province: Georgetown Region.||||||08-JUL-15
27355|Butlers Volcanic Group|23619|4|Described|p32 Table 1||Carboniferous|Previously Butlers Volcanics. Underlying Unit Einasleigh Metamorphics and Oak River Granodiorite - unconformable.||||||
27355|Butlers Volcanic Group|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27355|Butlers Volcanic Group|41272|5|Briefly described|p26|||See also M 1of 1 H05||||||21-MAY-15
27355|Butlers Volcanic Group|41680|5|Briefly described|p124|||Mention p106||||||21-MAY-15
27355|Butlers Volcanic Group|43113|4|Described|Table 1,p19.||Carboniferous|||||||
27355|Butlers Volcanic Group|43253|5|Briefly described|map legend||Carboniferous|||||||
27355|Butlers Volcanic Group|43259|6|Mentioned|Appendix 1,p4.||Carboniferous|||||||
27355|Butlers Volcanic Group|43286|5|Briefly described|Map Legend||Carboniferous|||||||
27355|Butlers Volcanic Group|43740|4|Described|p24|||||||||
27355|Butlers Volcanic Group|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Includes: Ballynure Rhyolite, Edmonds Creek Rhyolite, McLennons Creek Rhyolite. Of Lochaber Ring Structure.||||||08-NOV-04
27355|Butlers Volcanic Group|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Includes: Edmonds Creek Rhyolite, McLennons Creek Rhyolite.||||||
27355|Butlers Volcanic Group|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of Lochaber Ring Structure. Includes the Ballynure Rhyolite.||||||11-MAY-15
27355|Butlers Volcanic Group|63154|5|Briefly described|p285 Fig. 5|Carboniferous|Carboniferous|Geological province: Georgetown Inlier.||||||
27355|Butlers Volcanic Group|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Unit in Lochaber Ring Structure.|||Includes Edmonds Creek and McLennons Creek Rhyolites.||Rhyolitic ignimbrite and rhyolite lava.|
27355|Butlers Volcanic Group|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Lochaber Ring Structure, Kennedy Province.|||Includes Ballynure Rhyolite.||Rhyolitic ignimbrites.|
27355|Butlers Volcanic Group|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure.|||Includes McLennons Creek Rhyolite, Edmonds Creek Rhyolite, Ballynure Rhyolite.||Brown, crystal-poor to crystal-rich rhyolitic ignimbrite; brown to purple, sparsely porphyritic rhyolitic lava; pink, green or purple, crystal-rich rhyolitic ignimbrite with  abundant lithic clasts; purple, crystal-rich rhyolitic ignimbrite.|
27355|Butlers Volcanic Group|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
27355|Butlers Volcanic Group|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned.|||||Rhyolitic ignimbrites, rhyolitic-dacitic lavas and tuff; mostly minor to rare basalt and andesite.|
36160|Butterfly Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36160|Butterfly Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 269. I-Type.||||||
36160|Butterfly Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36160|Butterfly Granite|60425|5|Briefly described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, fine-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
77812|Butters Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Mainly fine to medium grained, even grained to porphyritic biotite granite; hydrothermally altered, porphyritic biotite granite, biotite microgranite.|
80075|Cadna-owie Formation, lower|67402|5|Briefly described|p26, p26 tbl RRM4, p115, p123|||Eromanga Basin. Maximum thickness of 130m. Demonstrated hydrocarbon seal.||||Overlies the Hooray Sandstone. Overlain by the Wyandra Sandstone Member, Cadna-owie Formation.|Coarsening upwards succession of mudstone, siltstone and sandstone up to 130m thick.|
24205|Calamia Member|22857|5|Briefly described|p318 Fig. 22.10A, p548 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). Siltstone, claystone, lithic-quartz arenite. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
24205|Calamia Member|23799|5|Briefly described|p48|||Of Koukandowie Formation [??].  Geological Province: Clarence-Moreton Basin.||||||28-SEP-05
24205|Calamia Member|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Gatton Sandstone.  Geological Province: Clarence-Moreton Basin.  Maximum thickness: 100m.||||||
24205|Calamia Member|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|39907|4|Described|p15|||||||||
24205|Calamia Member|41631|4|Described|p17|||See also Fig.2||||||
24205|Calamia Member|42248|2|Defined|App.1 p414|Early Jurassic||||||||
24205|Calamia Member|42463|6|Mentioned|Fig.3 P170|||||||||
24205|Calamia Member|43736|6|Mentioned|p29|||||||||
24205|Calamia Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
24205|Calamia Member|60281|5|Briefly described|p30, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Gatton Sandstone. Siltstone, claystone, sandstone.  Max. thickness: 100m.  Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60993|5|Briefly described|p6 Fig. 2, p18|||Of the Gatton Sandstone (Marburg Subgroup, Bundamba Group). . Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60995|4|Described|p64, p51 Fig. 3|Early Jurassic|Early Jurassic|Of the Gatton Sandstone. An overbank/floodplain facies of siltstone, claystone, sandstone - identified as a "shale break" in logs and drill cores. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60997|5|Briefly described|p140 Fig. 2|||Of the Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|60999|5|Briefly described|p169 Fig. 3|Early Jurassic|Early Jurassic|Basal member of the Gatton Sandstone. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6, p178 Fig. 10.||||||
24205|Calamia Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Gatton Sandstone (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
24205|Calamia Member|61006|5|Briefly described|p286|||Of the Gatton Sandstone.  Potential hydrocarbon seal - although it is predominantly siltstone and fine sandstone in some places and therefore will not act as a seal. ||||||
24205|Calamia Member|61310|5|Briefly described|Table C1 (p22-23)||Late Triassic|Of the Gatton Formation. Siltstone, claystone, lithic quartz sandstone. Max. thickness: 100m. Geological Province: Clarence-Moreton Basin||||||
24205|Calamia Member|67402|5|Briefly described|p187, p188, p190 fig CLM6, p190, p193|||Clarence-Moreton Basin. Deposited in a floodplain or braided stream environment. Between 10-20m thick. ||Gatton Sandstone. ||Overlies the Ripley Road Sandstone. Overlain by the Gatton Sandstone.|Shale interbedded with fine-grained sandstone.|
24205|Calamia Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 5-500m thick. Potential hydrocarbon seal. ||Gatton Sandstone||Overlies the Ripley Road Sandstone. Overlain by the Koreelah Conglomerate.|Siltstone, claystone and sandstone.|
24205|Calamia Member|69594|5|Briefly described|p544|||Clarence-Moreton Basin (NSW only). Numerous coastal outcrops.||Basal Gatton Sandstone.|||Shale and fine sandstone.|
36319|Calcifer Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36319|Calcifer Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A geophysical subdivision, described as a probable variant of this unit, is mapped separately.||Unit in Ootann Supersuite.|||Pale to white, or cream, fine- to medium-grained, even-grained to porphyritic, leucocratic (hornblende-)biotite granite; and white to pale pink aplite, locally with zones of pegmatite.|
25826|Calgoa Diorite|22845|6|Mentioned|p57||Triassic|||||||
25826|Calgoa Diorite|22846|4|Described|p6,7,66-7||Middle Triassic|Intrudes Native Creek Microdiorite.||||||
25826|Calgoa Diorite|24382|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|||||||
25826|Calgoa Diorite|41736|6|Mentioned|p119|||||||||
25826|Calgoa Diorite|41778|2|Defined|Table 3|Middle Triassic|Early Triassic|Described P376||||||
25826|Calgoa Diorite|41917|6|Mentioned|p523|||||||||
25826|Calgoa Diorite|42054|6|Mentioned|p273|||||||||
25826|Calgoa Diorite|43008|5|Briefly described|map legend|||||||||
25826|Calgoa Diorite|43588|6|Mentioned|p30|Late Triassic|Early Triassic|||||||
25826|Calgoa Diorite|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
25826|Calgoa Diorite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
25826|Calgoa Diorite|63821|4|Described|p17, p31|Middle Triassic|Early Triassic|Age: 234+/-2Ma (K-Ar biotite). Intrudes Gympie Group; intruded by Boonara Granodiorite+Boogooramunya Granite. Contact alteration zone occurs at contact with Gigoomgan Limestone. Hornblende-biotite granodiorite, augite-qtz microdiorite+hornblende tonalite.||||||07-FEB-11
25826|Calgoa Diorite|68679|5|Briefly described|p411, p428-430|Late Triassic|Late Triassic|Northern New England Orogen; Maryborough area. Generally poorly exposed, locally complex and heterogeneous.|234 +/- 2 Ma (K-Ar: Cranfield and Murray, 1989).|||Intrudes Native Creek Microgranite. Is intruded by Boonara Granodiorite and Boogooramunya Granite.|Hornblende diorite, biotite-hornblende diorite to granodiorite and minor granite. Later workers describe three different phases: hornblende-biotite granodiorite, hornblende tonalite and augite quartz microdiorite.|
29318|California Granite|23291|5|Briefly described|p101 Tb. 3.13|Early Permian|Late Carboniferous|Parent: California Creek Suite. Intrudes Martin Creek Microgranite, Mount Cardwell Granite (?). Age: 297Ma. Geological Province: Georgetown Region.||||||25-JUN-15
29318|California Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
29318|California Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 374. I-Type.||||||
29318|California Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29318|California Granite|23624|4|Described|p13|Permian|Carboniferous|Parent: Ootann Supersuite.||||||25-JUN-15
29318|California Granite|43087|6|Mentioned|p37|||Reserved as California Creek Adamellite.||||||25-JUN-15
29318|California Granite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
29318|California Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of California Creek Suite (Ootann Supersuite). I-type. White, medium-grained, slightly porphyritic to even grained biotite granite, with small quartz aggregates; extends into Georgetown region.||||||07-FEB-11
29318|California Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White, medium-grained, slightly porphyritic biotite monzogranite; with small quartz aggregates.|
29318|California Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White, medium-grained, slightly porphyritic biotite monzogranite; with small quartz aggregates.|
31781|Callamurra Member|13497|4|Described|iv, vi, viii, xii, p69 fig 6.1|Early Triassic|Late Permian|Cooper Basin. Informally defined by Channon and Wood (1989). A reference section was assigned by Channon and Wood (1989). Maximum drilled thickness of 150m in Moomba Field. Deposited in a fluvial floodplain environment. Regarded as a regional oil and gas seal unit. Hosts economic oil and gas reservoirs in places. Seal and reservoir characteristics discussed. See also p104-p110, p157 tbl 10.1, p159, p161, p165, p166 fig 10.8.||Arrabury Formation||Conformably overlies the Toolachee Formation. Disconformably overlain by the Paning Member. Overlain by the Wimma Sandstone Member.|Siltstone and mudstone beds with minor sandstone interbeds.|
31781|Callamurra Member|13516|5|Briefly described|p171 fig 12|Early Triassic||In Eromanga Basin.||Of Arrabury Formation||||
31781|Callamurra Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation||||||
31781|Callamurra Member|23155|6|Mentioned|Fig 8 on p16|Triassic|Permian|||||||
31781|Callamurra Member|23375|4|Described|Fig2 p265,280|Dorashamian|Dzhulfian|Of the Arrabury Formation.Geological Province: Cooper Basin.||||||30-JUN-08
31781|Callamurra Member|24210|5|Briefly described|p133 Fig. 2|Early Triassic|Late Permian|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
31781|Callamurra Member|44133|5|Briefly described|p65 Fig. 8.3, 85|Triassic|Permain|Of the Arrabury Formation. Geological Province: Cooper Basin. ||||||
31781|Callamurra Member|60717|5|Briefly described|p40 Fig. 2|Scythian|Tatarian|Of Arrabury Formation (Nappamerri Group). Overlies Toolachee Formation; overlain by other members of the unit - Paning and Wimma Sandstone Members.  Thickness: 125m. Geological Province: Cooper Basin.||||||31-JAN-08
31781|Callamurra Member|61015|6|Mentioned|p44|||Of the Birkhead Formation?  Contains gas.||||||19-APR-05
31781|Callamurra Member|61613|5|Briefly described|p282 Fig. 2|Late Permian|Late Permian|Of Arrabury Formation. Overlain by Paning Member. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
31781|Callamurra Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Of Arrabury Formation. Geological Province: Cooper Basin.||||||31-MAR-09
31781|Callamurra Member|62537|6|Mentioned|p191 Fig.2. |Early Triassic|Early Triassic|Cooper Basin.||Unit in Arrabury Formation.||||
31781|Callamurra Member|62730|5|Briefly described|p352 Fig. 1|Early Triassic|Late Permian|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
31781|Callamurra Member|63978|2|Defined|p7, p19-20, Fig. 3|Early Triassic|Late Permian|Basal member of Arrabury Fm (Nappamerri Gp). Conformable on Toolachee Fm; overlain by Paning Mbr (disconformably in places). Max.thickness: 170m. In Cooper Basin. Lower carbonaceous mudst.+ siltst., overlain by interbedded mudst.+ siltst.+ lesser sst.||||||07-FEB-11
31781|Callamurra Member|64048|5|Briefly described|p67|||Within the lower Arrabury Formation. Contains a sandstone gas reservoir ~10m thick. Dominantly sandstone and mudstone - interbedded siltstones, mudstones and very fine-grained sandstones.||||||07-FEB-11
31781|Callamurra Member|64197|6|Mentioned|p625 Fig.1c|Early Triassic|Late Permian|Cooper Basin.||||Underlies the Paning Member; overlies the Toolachee Formation.||
31781|Callamurra Member|64665|5|Briefly described|p53 Fig.2.|Early Triassic|Early Triassic|Cooper Basin.||Basal unit in Arrabury Formation.||||
31781|Callamurra Member|65489|5|Briefly described|p48, p96, p131-132|Scythian|Tatarian|125m thick. Regarded as a regional seal; also contains economic oil and gas reservoirs locally, and is a leaky seal elsewhere.||Basal unit in Arrabury Formation.||Overlies Toolachee Formation (Gidgealpa Group). Is overlain by Paning and Wimma Sandstone Members.||
31781|Callamurra Member|67402|5|Briefly described|p90 fig CPR4, p91 tbl CPR1|||Deposited in floodplain and shallow perennial lacustrine environments. Maximum thickness of 170m. See also p90-p94, p98, p100, p101 tbl CPR2, p103, p303.||Arrabury Formation||Conformably overlies the Toolachee Formation. Conformably overlain by the Paning Member.|Mudstone and siltstone sequence with minor fine to medium-grained sandstone interbeds.|
31781|Callamurra Member|68731|5|Briefly described|p200 Fig 3.110, p207|Early Triassic|Lopingian|Also mis-spelt as the Calamurra Member on p207. Includes rocks assigned to the lower Paning Member by Powis (1989). Flood plains and shallow perennial lakes, with input from meandering streams. Includes late Lopingian-early Triassic palynofloras.||Of the Arrabury Formation.||Conformably underlain by the Toolachee Formation. Unconformably underlain by the Innamincka Formation. Overlain by the Paning Member (possible disconformity).|Carbonaceous mudstone and siltstone, which grade up into organically lean, partly mottled mudstone and siltstone, with lesser fine to medium, moderately sorted quartzose, in part micaceous sandstone with an argillaceous and siliceous matrix.|02-JUL-14
31781|Callamurra Member|69797|5|Briefly described|p17 Fig.2|Early Triassic|Late Permian|Age: Tatarian - Scythian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
31781|Callamurra Member|69946|5|Briefly described|p9, p36, p54|Early Triassic|Permian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning Member.||
31781|Callamurra Member|69947|5|Briefly described|p13 Fig.7.2|Early Triassic|Permian|Cooper Basin.||Arrabury Formation.||||
31781|Callamurra Member|70317|6|Mentioned|p33|Early Triassic|Late Permian|Cooper Basin.||Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning, and Wimma Sandstone, Members.||
31781|Callamurra Member|70823|5|Briefly described|p40, p75, p79, p81, p82|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlain by the Wimma Sandstone Member.|Thin fine to medium grained quartzose sandstones.|
31781|Callamurra Member|70824|4|Described|p7, p104|Induan|Induan|Cooper Basin. Deposited in floodplains, lacustrine environments and moderate sinuosity fluvial environments.||Arrabury Formation||Overlies the Toolachee Formation. Unconformably overlain by the Paning Member.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
31781|Callamurra Member|70946|5|Briefly described|p1089|Early Triassic|Permian|Cooper Basin. Deposited in a floodplain, lacustrine or moderate sinuosity fluvial channel environment.||Arrabury Formation.||Unconformably overlain by Paning Member.||08-OCT-18
31781|Callamurra Member|71265|5|Briefly described|p589|Induan|Induan|Cooper Basin.||Arrabury Formation.||Overlies Toolachee Formation. Is overlain by Paning Member.||
31781|Callamurra Member|71342|6|Mentioned|Ch5 p9, Ch5 p54, Ch7 p13|Scythian|Tatarian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in floodplain, lacustrine or fluvial channel environments.||Arrabury Formation||Overlies the Toolachee Formation. Overlain by the Paning Member.||
31781|Callamurra Member|71701|5|Briefly described|p155|Olenekian|Induan|Cooper Basin.||Arrabury Formation||Unconformably overlain by the Paning Member.||
31781|Callamurra Member|72297|5|Briefly described|p742|||Cooper Basin; absent in the E and N areas. Acts as a regional seal.||Basal Arrabury Formation.||||
31781|Callamurra Member|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin. Contains gas.||Nappamerri Group||||
31781|Callamurra Member|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Panning Member, Wimma Sandstone Member and Tinchoo Formation, shown as floodplain, lacustrine, fluvial channels. Gas.||||||
31781|Callamurra Member|73251|6|Mentioned|p62|Early Triassic|Permian|Cooper Basin. Lacustrine and moderately sinuous fluvial channel depositional environments. Contains[?] gas.||Arrabury Formation, Nappamerri Group||Underlain by Toolachee Formation (Gidgealpa Group). Overlain by Arrabury Formation including Callamurra Member.||
31781|Callamurra Member|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin. Hosts gas.||Nappamerri Group||Underlain by Toolachee Formation. Overlain by Panning Member.||
31781|Callamurra Member|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment.|ca 245 Ma|Nappamerri Group||Overlies Toolachee Formation, underlies Panning Member||
79123|Calton Andesite Member|70913|4|Described|p8 fig 3, p10, p32-p25, p67 fig 9|Middle Permian|Early Permian|Gympie Province. Named for the Calton Terrace of Calton Hill. Discussed as a Member of the Rammutt Formation but  abbreviated to Calton Andesite p51. See also Calton Andesite clastic facies App 1 maps. Up to 60m thick. Lithologically similar to the Kidgell Andesite Member. Mineralogy, distribution and geochemistry are briefly discussed. Replaces both company informal names Calton clastics/Clastics (p8, 10,12) and Calton volcanics/Volcanics/Andesite (p8, 10, 12).||Rammutt Formation|Includes the Calton clastic facies.|Overlies the Eldorado Clastics. Overlain by the Nash Clastics.|Massive, greenish-grey, feldspar-phyric andesite lava that is characterised by distinctive euhedral plagioclase phenocrysts.|15-SEP-17
79123|Calton Andesite Member|73197|6|Mentioned|p477 Tb.3|Lopingian|Cisuralian|New England Orogen, northern. U-Pb zircon age from Li et al., (2015).|275-255 Ma U-Pb zircon|Rammutt Formation||||
77875|Calvert Supersequence|67539|6|Mentioned|p3|||||||||
36487|Cambridge Creek microgranite|23291|4|Described|p98 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Purkin Batholith intruding the Etheridge Group. Age: 311+/-5Ma (K-Ar, Richards et al). Geological Province: Georgetown Region.||||||08-JUL-15
36487|Cambridge Creek microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 66.  Assumed to be I-Type.||||||
31368|Cambroon beds|22845|2|Defined|p42,3,70,2-4,6,9,82|Permian|Permian|Formerly part of the Amamoor beds. Possible correlation to Cedarton Volcanics.||||||22-OCT-08
31368|Cambroon beds|22846|6|Mentioned|p47||Permian|Intruded by Tungi Creek Granodiorite.||||||
31368|Cambroon beds|23251|6|Mentioned|p19, o36|||||||||21-JUN-06
31368|Cambroon beds|23542|5|Briefly described|Fig 1 p378|||Also see p377.||||||
31368|Cambroon beds|23799|5|Briefly described|p125|Early Permian|Early Permian|Mafic and lesser felsic volcanics and coarse clastics.  Geological Province: North D'Aguilar Subprovince.||||||
31368|Cambroon beds|43588|6|Mentioned|p31||Late Carboniferous|||||||
31368|Cambroon beds|44925|5|Briefly described|Map Legend||Permian|||||||
31368|Cambroon beds|61780|6|Mentioned|p255, 256, p259, p264|||||||||
31368|Cambroon beds|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with the Marumba and Northbrook beds; the Cedarton Volcanics, and the Kandanga Creek Megabreccia, are all mapped under the symbol, Pn.||||||
31368|Cambroon beds|68679|5|Briefly described|p321, p324-326, p331, p384-385|Permian|Permian|Sliwa et al. (1993). Cressbrook Basin, North D'Aguilar Subprovince, northern New England Orogen. Occurs as a narrow NW-trending wedge a few kilometres wide extending 30km SE from near Kenilworth. Early Permian fossils necessitated removing it from the (Mississippian) Amamoor beds. Cover basin sediments. The mafic volcanics include a single unit of calcite-filled vesicular basalt, and pebbly andesitic volcaniclastic rocks. Deformations described. Is correlated with Cedarton Volcanics; probably also with Marumba beds and Kandanga Creek Megabreccia.||||Unconformably overlies Amamoor beds. Is overlain unconformably by North Arm Volcanic Group. Is faulted against Booloumba beds. Is intruded by Tungi Creek Granodiorite and Neurum Complex.|Mudstone, locally calcareous sandstone, pebble conglomerate and pebbly sandstone; common hematitic siltstone with graded bedding, radiolarians and dispersed fragments of quartz and chert; and minor mafic volcanics.|
76891|Camel Creek Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Pink, fine to medium grained, equigranular, moderate to strongly foliated granite; small scattered mafic xenoliths common; locally cut by quartz reefs.|
76891|Camel Creek Granite|69591|6|Mentioned|p60||||||||Pink, fine- to medium-grained, equigranular, moderately to strongly foliated granite; small scattered mafic xenoliths common; locally cut by quartz reefs.|
35184|Cameron Creek Granite|23042|4|Described|p87,8, Fig 2|Cretaceous|Jurassic|||||||
35184|Cameron Creek Granite|60473|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of the Urannah Batholith. Dark pink, medium grained, leucocratic titanite-hornblende-biotite monzogranite.||||||17-SEP-04
35184|Cameron Creek Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35184|Cameron Creek Granite|65388|3|Fully described|p406-407, p403 Fig. 135|Cretaceous|Cretaceous|Interpreted to intrude Carmila beds. Probable age given. Dominantly dark pink, fine to medium-grained, uneven-grained to slightly porphyritic biotite-hornblende monzogranite boulders in type area.||||||
68909|Camooweal Dolostone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: central Georgina Basin||||||
68909|Camooweal Dolostone|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Pale microbial dolostone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Pale microbial dolodstone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Dolostone, dolomitic limestone, planar microbial doloaminite with nodular chert; minor marl; basal intraclast and ooid dolograinstone.||||||
68909|Camooweal Dolostone|64068|5|Briefly described|p62, 63, 128, 225|||Western and central Georgina Basin. Correlated with Arthur Creek Formation, Blazan Shale, Inca Formation, Quita Formation. The Cambrian succession in Lake Nash 1 borehole (central Georgina Basin) (1962) was attributed to this unit. Oils and tar were present in recovered cores.||||||24-MAR-16
68909|Camooweal Dolostone|64443|1|Redefined|p2, p5 Fig.3, p6 Tb.1, p14-22, p40-41 |Mindyallan||Note: revised definition. Formerly Camooweal Dolomite (Opik, 1954, 1956). Of Barkly Group. Extensive unit across central and east Georgina Basin. Laterally interdigitates with Age Creek Formation. Correlative with Anthony Lagoon beds (possibly), Age Creek Formation, V Creek Limestone, Mail Change Limestone, Devoncourt Limestone and/or Roaring Siltstone, upper Arthur Creek Formation. Max 167+m thick. Erosion by Gregory River is producing deep gorges.||||Conformably overlies Ranken Limestone, Wonarah Formation, Currant Bush Limestone; conformably underlies Arrinthrunga Formation; unconformably underlies Brunette Limestone and Austral Downs Limestone.|Dolostone, minor marl and quartz sandstone; basal intraclast, ooid and oncoid dolostone and quartz sandstone. Has spheroidal chert concretions, microbial lamination, stromatolites. Essentially unfossiliferous.|14-MAY-14
68909|Camooweal Dolostone|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Barkly Group, Georgina Basin . Overlies Ranken Limestone, underlies Brunette Limestone. Pale microbial dolostone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|65337|4|Described|p9 Fig.5.|Middle Cambrian|Middle Cambrian|Southwest MOUNT DRUMMOND area. 167 + m thick.||Unit in Barkly Group.||Overlies Ranken Limestone, Currant Bush Limestone, Wonarah Formation. Is overlain by Arrinthrunga Formation.|Pale microbial dololaminite with nodular chert, dolosparstone; minor peloid and ooid dolostone, conglomerate, dolomitic limestone, marl; lower high-energy interval of quartzic, intraclast and ooid dolograinstone and quartz sandstone.|
68909|Camooweal Dolostone|65344|5|Briefly described|p3 Fig. 2, p37-42|Early Cambrian|Early Cambrian|Of the Undilla Sub-basin, Georgina Basin.||||Overlies Wonarah Formation or Ranken Limestone.||
68909|Camooweal Dolostone|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||||Overlies Ranken Limestone.||
68909|Camooweal Dolostone|67352|6|Mentioned|p21|||||||Overlies Wonarah Formation.||
68909|Camooweal Dolostone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2. High-energy barrier and protected back barrier deposits.||||Overlies Ranken Limestone, Wonarah Formation, Currant Bush Limestone.|Carbonate rocks.|12-JUL-16
68909|Camooweal Dolostone|69443|4|Described|p28:16, 20-25, 33|Middle Cambrian|Middle Cambrian|Opik (1954, 1956). Central Georgina Basin. Unfossiliferous. Forms prominent hills to low rubbly outcrops; exposures are commonly significantly silicified. Notionally 240-300m thick, but usually less than 200m. Interdigitates with Age Creek Formation and Ranken Limestone. Also correlated with V-Creek, Mail Change, Devoncourt Limestones; Roaring Siltstone, Arthur Creek Formation and possibly Anthony Lagoon Formation. Age from surrounding units. Displays a prominent isolated fold: the Lake Nash Anticline.||Barkly Group.||Transitionally overlies and is partial lateral equivalent of Currant Bush Limestone. Conformably overlies Wonarah Formation and Ranken Limestone. Is overlain conformably by Arrinthrunga Formation.|Lower high-energy interval of dolostone, dolomitic limestone with nodular chert, minor marl and quartz sandstone; overlain by lower-energy microbial dololaminite with thin bands of intercalated dolomudstone, with local intraformational conglomerates.|12-JUL-16
68909|Camooweal Dolostone|69445|6|Mentioned|p30:17|||||||Overlies Colless Volcanics.||12-JUL-16
68909|Camooweal Dolostone|69446|6|Mentioned|p31:4|||Georgina Basin.||||||12-JUL-16
68909|Camooweal Dolostone|69561|6|Mentioned|p32 fig 1, p34|Boomerangian|Undillan|||||Conformably overlies Ranken Limestone, Wonarah Formation|Intraclast grainstone, oncoid rudstone and quartz sandstone.|
68909|Camooweal Dolostone|69591|4|Described|p88, p96|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. 100-200m thick in drill cores. Basal, high-energy peritidal to shallow subtidal barrier environment, passing upwards into restricted to epeiric back-barrier. Maximum age is middle Cambrian Ptychagnostus gibbus Zone. Unfossiliferous. Coeval with Age Creek Formation, V-Creek Limestone and Mail Change Limestone.||Barkly Group.||Conformably overlies Ranken Limestone and Wonarah Formation.is overlain ("apparently") by Arrinthrunga Formation. Interdigitates with Age Creek Formation.|Dolostone with minor marl, quartz sandstone and basal intraclast, ooid and oncoid dolostone and quartz sandstone.|
68909|Camooweal Dolostone|69673|5|Briefly described|p116, p117|||300m thick.||Barkly Group|||Dolostone, dolomitic limestone, nodular chert, minor marl.|
68909|Camooweal Dolostone|70380|6|Mentioned|p745, p759|Series 3|Series 3|Undilla Sub-basin, Georgina Basin.||||||
68909|Camooweal Dolostone|72516|6|Mentioned|p92|Cambrian|Cambrian|Western and central Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
68909|Camooweal Dolostone|72919|6|Mentioned|p77|||||||||
68909|Camooweal Dolostone|73083|6|Mentioned|p10, p75|middle Cambrian|middle Cambrian|||||Overlain by Arrinthrunga Formation and Ninmaroo Formation.|Includes dolostone, marl, and quartz sandstone.|
33146|Camp Creek Granite|23042|4|Described|p15,26,68, Fig 2||Carboniferous|Intrudes the Connors Volcanics. Overlying unit Leura Volcanics.||||||28-MAY-08
33146|Camp Creek Granite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Pink, medium to coarse grained biotite granite; subordinate pink microgranite and granophyre near margins.||||||
33146|Camp Creek Granite|61035|5|Briefly described|p10 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Broadsound and Clive Creek Volcanics. Geological Province: Connors Sudprovince. Pink, medium to coarse-grained biotite granite; subordinate pink microgranite and granophyre near margins.||||||07-FEB-11
33146|Camp Creek Granite|65388|2|Defined|p354-355, p86, 89, 94, 95, 101, 102,399|Late Carboniferous|Late Carboniferous|Connors Arch pluton. Intruded and hornfelsed Clive Creek Volcanics, Broadsound Range Volcanics. Probably overlain by the Leura Volcanics. Probable age given. Mainly pink, coarse-grained, equigranular biotite granite. Some microgranite, granophyre along margins.||||||
33146|Camp Creek Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Dacey, Olympus,Toobier, Tooloombah Creek and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
33146|Camp Creek Granite|68679|5|Briefly described|p347, p356|Carboniferous|Carboniferous|Northern New England Orogen.||||Intrudes the Broadsound Range Volcanics.||
36290|Camp Oven Dacite|23291|4|Described|p93 Table 3.9|Early Permian|Early Permian|Parent: Galloway Volcanic Group. Age: 290+3Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36290|Camp Oven Dacite|23510|5|Briefly described|Map Legend||Early Permian|of Galloway Volcanic Group.||||||
38246|Camp Oven Mountain Complex|23422|5|Briefly described|p218 Table 6.12|||||||||
38246|Camp Oven Mountain Complex|69593|5|Briefly described|p494-495|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. Commonly associated with intrusives of the Leichhardt Supersuite.|~310-283 Ma.|Tuckers Suite (?).|||Rhyolitic and dacitic ignimbrite; rare andesitic ignimbrite and lava, and andesitic to rhyolitic volcaniclastics. I-type.|
27732|Campaspe Formation|22621|6|Mentioned|p204||Tertiary|||||||
27732|Campaspe Formation|22713|5|Briefly described|p125|Quaternary|Miocene|||||||
27732|Campaspe Formation|22937|4|Described|p203 fig1|Pleistocene|Pliocene|Age: 1.3-3.5Ma.||||||
27732|Campaspe Formation|23049|5|Briefly described|p37|Quaternary|Tertiary|||||||
27732|Campaspe Formation|23318|5|Briefly described|p393|Tertiary|Tertiary|||||||07-FEB-07
27732|Campaspe Formation|23422|4|Described|p186, p204 Table 6.3|Pliocene|Pliocene|Formerly Campaspe Beds. Maximum thickness: 120m.||||||
27732|Campaspe Formation|23424|6|Mentioned|p340|||Charters Towers Area.||||||
27732|Campaspe Formation|23430|4|Described|p504 Table 14.5|||Also see p527. Underlying Unit Balfes Creek beds. Kalpowar Basin Province.||||||
27732|Campaspe Formation|23431|5|Briefly described|p538|||||||||
27732|Campaspe Formation|23499|5|Briefly described|map legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|23505|5|Briefly described|Map legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|23508|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|23509|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|23619|6|Mentioned|p14|||||||||
27732|Campaspe Formation|23893|4|Described|p22|Pliocene|Pliocene|||||||
27732|Campaspe Formation|23940|5|Briefly described|p917 Fig. 3|Tertiary|Tertiary|Formation is Fm. in text.  Geological Province: Mount Windsor subprovince.||||||
27732|Campaspe Formation|23952|5|Briefly described|p1176 Fig.1|Tertiary|Tertiary|Geological Province: Mount Windsor subprovince||||||
27732|Campaspe Formation|23986|4|Described|p89|||Geological Province: Drummond Basin.||||||
27732|Campaspe Formation|23988|4|Described|p40|Tertiary|Tertiary|Geological Province: Drummond Basin.||||||
27732|Campaspe Formation|24035|5|Briefly described|p2, p5, p7 Fig. 4b, p11|Tertiary|Tertiary|Underlain by Trooper Creek Formation.||||||
27732|Campaspe Formation|24036|5|Briefly described|p2, p3 Fig. 1, p12|Tertiary|Tertiary|Overlies Paleozoic basement rocks. Geological Province: North Drummond Basin. Sedimentary rocks.||||||
27732|Campaspe Formation|41244|4|Described|p30|||Formerly Campaspe Beds.||||||06-MAY-09
27732|Campaspe Formation|41774|6|Mentioned|p33|||||||||
27732|Campaspe Formation|42633|5|Briefly described|Table 1 P6|||||||||
27732|Campaspe Formation|42933|6|Mentioned|p238|||||||||
27732|Campaspe Formation|43687|5|Briefly described|p203,204|Pleistocene|Pliocene|||||||
27732|Campaspe Formation|43758|6|Mentioned|p497||Tertiary|||||||
27732|Campaspe Formation|43933|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|43934|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
27732|Campaspe Formation|50153|4|Described|p1, 4, 9,13-16,18, 20-24|Pleistocene|Pliocene|Possible Pliocene/Pleistocene age based on stratigraphic relationship between two basalt flows with isotopic ages of 3.8 and 1.35 Ma. Younger than Suttor and Southern Cross Formations|||||Poorly sorted, clay cemented sandstones and siltstones with minor conglomerate.|
27732|Campaspe Formation|61155|5|Briefly described|p20|Early Pliocene|Early Pliocene|Overlies Allingham Formation. Thickness: 10m. In the Townsville area.||||||
27732|Campaspe Formation|61814|5|Briefly described|p18, p25|Tertiary|Tertiary|Dominated by sand, with minor interbedded silt and clay. Partly overlies the Southern Cross Formation (Red Falls area). Geological Province: Drummond Basin.||||||08-FEB-10
27732|Campaspe Formation|61829|5|Briefly described|p174, p175|Cenozoic|Cenozoic|Lightly weathered gravel to sand sediments.||||||09-JUN-06
27732|Campaspe Formation|61848|6|Mentioned|p304|||Unit in Queensland.||||||
27732|Campaspe Formation|64849|5|Briefly described|Map legend|Quaternary|Tertiary|Age is Late Tertiary to Quaternary. Kaolinitic quartz sandstone, conglomerate, mudstone, variegated mudstone and siltstone.||||||
27732|Campaspe Formation|64850|5|Briefly described|Map legend|Quaternary|Tertiary|Poorly consolidated sandstone, claystone, conglomerate and dicontinuous nodular ferricrete.||||||09-FEB-09
27732|Campaspe Formation|69599|5|Briefly described|p580, p593-594, p603|Pliocene|Pliocene|Wyatt et al. (1970). A thin (mostly <30m, up to 150m), extensive, flat-lying unit across >8000 km2. Erosive channel fill deposits followed by fluvial sheet deposition. Unfossiliferous. Age from enclosing units.||||Overlies Myrrlumbing Basalt. Is overlain by Hann Creek Basalt. May be correlated with Yam Creek and Falloch beds.|Immature sandstone, pebbly sandstone and minor siltstone interbeds, with detritus from adjacent basement provinces. Upper surface is commonly ferruginised (Campaspe Surface).|
27732|Campaspe Formation|69789|5|Briefly described|p1041-1059|Pliocene|Pliocene|Charters Towers region, north Queensland. Covers 11,000 km2. Average thickness 60m; maximum over 200m. The unit blankets a featureless bedrock pediment plain. Clay cement produces poor permeability: productive water bores are very rare. Texture and mineralogy, depositional model and environment are discussed in detail.||||Disconformably overlies Southern Cross Formation. Is interlayered with, and overlain by, Nulla Basalt.|Poorly sorted sandstone, minor conglomerate and siltstone; contains paleosol horizons with associated calcrete.|
27732|Campaspe Formation|73115|5|Briefly described|p25, 75-78, 80, 94, 97, 100, 102, 131...|||Northern portions represent sedimentation in sub-distal to distal zones of the Nulla Basalt Province. Extensive to the south of the province. There are some areas where the unit is not underlain by / interbedded with basalt units. Also on p: 90, 94, 99, 105, 110, 115, 120; App.B p153, p159-160. Also misspelt as Campapse Formation p77.||||Underlain by Bluff Downs Basalt and Southern Cross Formation. Interfingers with Myrrlumbing Basalt. Overlain by Hann Creek Basalt.|Consists mostly of fluvial sediments interbedded with basalts.|
27732|Campaspe Formation|75060|6|Mentioned|p42|Pliocene|Pliocene|NE QLD.|||||Predominance of vermiculite and smectite-rich illite/smectite mixed-layer clays.|
75127|Campbell Creek Granodiorite|60425|3|Fully described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. Grey, fine-grained granodiorite; I-type. Not assigned to a Suite.||||||07-FEB-11
36285|Campbell Mountain Granite|23291|5|Briefly described|p97 Tb. 3.11|Early Permian|Early Permian|Parent: Kangaroo Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
36285|Campbell Mountain Granite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36285|Campbell Mountain Granite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Kangaroo Creek Supersuite.||||
36244|Campsbourne Granodiorite|23503|5|Briefly described|Map Legend||Late Carboniferous|of Almaden Supersuite.||||||
29557|Campwyn Volcanics|22604|6|Mentioned|p437|||||||||
29557|Campwyn Volcanics|22800|6|Mentioned|Fig.14 p592, 593|Visean||||||||
29557|Campwyn Volcanics|23042|3|Fully described|p10,111|Carboniferous|Devonian|||||||
29557|Campwyn Volcanics|23162|5|Briefly described|p885|Early Carboniferous|Middle Devonian|Back/Forearc Deposit.||||||
29557|Campwyn Volcanics|23468|6|Mentioned|p 293|||||||||
29557|Campwyn Volcanics|24399|5|Briefly described|p286, p279 Fig. 4|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
29557|Campwyn Volcanics|24467|2|Defined|p379|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||21-OCT-08
29557|Campwyn Volcanics|42979|2|Defined|p300|Early Carboniferous|Middle Devonian|Supersedes Campwyn beds of Jenson et al (1966).||||||
29557|Campwyn Volcanics|42980|4|Described|p303|||||||||
29557|Campwyn Volcanics|60445|5|Briefly described|p4|Early Carboniferous|Middle Devonian|Complex unit of shallow marine to subaerial pyroclastic to volcaniclastic flows and lavas, minor limestone, shallow intrusions, non-volcanic siliciclastic rock and ignimbrite.||||||02-JUL-14
29557|Campwyn Volcanics|60473|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Sandstone, siltstone, mudstone, breccia, hyaloclastite, rhyolitic ignimbrite; minor conglomerate, lapilli tuff, limestone.||||||
29557|Campwyn Volcanics|60705|5|Briefly described|p645|Famennian|Frasnian|Silicic volcanics. Age: ca 360-350Ma. Geological Province: northern New England Fold Belt.||||||11-APR-05
29557|Campwyn Volcanics|60787|5|Briefly described|p9|Carboniferous|Devonian|||||||
29557|Campwyn Volcanics|61035|6|Mentioned|p12, p13|Early Carboniferous|Late Devonian|Geological Province: Yarrol Province. This unit is now re-assigned to the Rockhampton Group.||||||07-FEB-11
29557|Campwyn Volcanics|61916|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Sandstone, siltstone, mudstone, (locally with radiolarians), pebbly sandstone, breccia, mafic hyaloclastite, rhyolitic ignimbrite; minor conglomerate, lapilli tuff, limestone. Overlain by Whitsunday Volcanics.||||||
29557|Campwyn Volcanics|63832|6|Mentioned|p131 fig 2|Carboniferous|Carboniferous|Of east Bowen Basin.||||||
29557|Campwyn Volcanics|64315|5|Briefly described|p525|Early Carboniferous|Early Carboniferous|Geological province: Drummond Basin. Open marine sediments.||||||21-OCT-08
29557|Campwyn Volcanics|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Carboniferous|Northern New England Fold Belt. Shown with Rockhampton Group. Includes some biostratigraphic and some radiometric age control. ||||||
29557|Campwyn Volcanics|64783|5|Briefly described|p86|||Contains a large number of inherited zircons of 380-370 Ma (Bryan et al.,2004).||||||15-NOV-17
29557|Campwyn Volcanics|65388|3|Fully described|p58-69; p443, p59, 61, 63, 72, 92|Tournasian|Late Devonian|Of Campwyn Subprovince, Yarrol Province.  Formalised to Campwyn Volcanics by Fergusson and others (1994) but no type section. Faulted against Mountain View Volcanics, Carmila beds. May be unconformably overlain by Carmila beds. Intruded by dykes dated as Early Permian (~275 Ma). Include Late Devonian to Tournaisian fossils in limestone parts. Abundant coarse-grained volcaniclastic and volcanic rocks, along with siliceous sandstone, siltstone, mudstone, limestone and intrusive rocks. See also , 94, 232, 407, 441, 447.||||||
29557|Campwyn Volcanics|65706|4|Described|Tb.1 (p13,15,18,19); p50, p62|Early Carboniferous|Middle Devonian|Upper part of this unit is equivalent to Edgecumbe beds; intruded by small plugs of Cape Hillsborough beds; unconformably underlies and is faulted against Cape Hillsborough beds. Hosts gold mineralisation at Mackay Prospect. Also called Campwyn beds on p50, p62.||||Probably unconformably underlies Carmila beds.|Acid to intermediate flows and pyroclastics, siltstone, mudstone (locally with radiolarians), quartzose to pebbly sandstone, breccia, mafic hyaloclastite, with minor conglomerate, oolitic limestone.|
29557|Campwyn Volcanics|68358|5|Briefly described|p6-8, p19|Early Carboniferous|Late Devonian|Basement to the Hillsborough Basin; crops out along the SE margin. Enriched in U, Th and K, suggesting the unit may be heat producing.||||Correlative of Edgecumbe Beds.|Felsic to intermediate volcanic flows and pyroclastics, and shallow-marine to fresh-water sediments.|
29557|Campwyn Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Campwyn Subprovince. This unit is mapped with the Edgecumbe beds under the symbol, DCw.||||||
29557|Campwyn Volcanics|68679|5|Briefly described|p336, p338, p346-349, p360, p363-364|Mississippian|Late Devonian|Jensen et al. (1966); Clarke et al. (1971) and others (listed). Campwyn Subprovince, Yarrol Province. A narrow belt extends ~180km along the coast N and S of Mackay and up to 10km inland. Environment of deposition and age determinations discussed: several geochronological age determinations given.|373.6 +/- 2.9 Ma to 354.3 +/- 4.1 Ma.|||Is overlain by Neerkol Formation. May correlate with Tanderra Volcanics.|Basaltic lavas and high-level intrusions, coarse-grained volcaniclastic rocks with lesser lithic sandstone and siltstone; a silicic facies includes ignimbrite, accretionary lapilli tuff, sandstone, rare syn-sedimentary intrusions and limestone.|
29557|Campwyn Volcanics|68731|6|Mentioned|p177 Fig 3.91|||||||||
29557|Campwyn Volcanics|68822|5|Briefly described|p337|||Yarrol Belt. Displays an upwards change in composition from mafic to felsic in the late Devonian and into the early Carboniferous.||||||
29557|Campwyn Volcanics|68901|6|Mentioned|p2 Fig. i, p3|Early Carboniferous|Late Devonian|||||||26-SEP-18
29557|Campwyn Volcanics|69582|5|Briefly described|p41, p43-p45|Early Carboniferous|Late Devonian|Campwyn Subprovince. Outcrops along the southeastern margin of the Hillsborough Basin.||||Broadly equivalent to the Edgecumbe beds.|Felsic to intermediate volcanic flows and pyroclastics and shallow marine to fresh-water sedimentary sequences.|
29557|Campwyn Volcanics|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|||||||
29557|Campwyn Volcanics|70740|6|Mentioned|p5|||Drummond Basin. ||||||
29557|Campwyn Volcanics|73179|6|Mentioned|p1152|Visean|Famennian|East of Adavale Basin. Geochron from Bryan et al. (2004).|ca 360-340 Ma|||||
29557|Campwyn Volcanics|73197|5|Briefly described|p465 Fig.4, p467-468|Carboniferous|Carboniferous|New England Orogen, northern. Campwyn Subrovince. Forearc basin with extensive arc-proximal rocks. Range of zircon inheritance in ignimbrites attributed to anatectic melting and reworking of continental crust (Bryan et al., 2004).|||||Basaltic lavas and silicic tuffs and ignimbrites.|
29557|Campwyn Volcanics|73570|6|Mentioned|p916, p918|Carboniferous|Devonian|Yarrol Belt.||||||
25687|Candlow Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with Willyama Supergroup Bijerkerno Metasediments and Mt Isa Soldiers Cap Group.||||||19-JUN-13
25687|Candlow Formation|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon). Thickness: 1000-3500 m. Geological Province: Georgetown Region.||||||25-JUN-15
25687|Candlow Formation|23430|5|Briefly described|p456.|||Of Etheridge Group.||||||
25687|Candlow Formation|23431|5|Briefly described|p530|||Forsayth Subprovince.||||||
25687|Candlow Formation|24197|5|Briefly described|p77|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
25687|Candlow Formation|35921|2|Defined|p39|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||25-JUN-15
25687|Candlow Formation|36153|5|Briefly described|p63|||||||||
25687|Candlow Formation|36216|6|Mentioned|p208|||||||||
25687|Candlow Formation|36780|5|Briefly described|p8|||||||||
25687|Candlow Formation|36937|6|Mentioned|p229|||||||||
25687|Candlow Formation|37448|4|Described|p43|||||||||
25687|Candlow Formation|37570|4|Described|p116|||See also Fig.2 and P125||||||
25687|Candlow Formation|38714|6|Mentioned|p182|||||||||
25687|Candlow Formation|38716|4|Described|p193|||||||||
25687|Candlow Formation|39445|5|Briefly described|Table 2|||||||||
25687|Candlow Formation|39566|6|Mentioned|p51|||||||||
25687|Candlow Formation|39687|6|Mentioned|p1|||||||||
25687|Candlow Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
25687|Candlow Formation|39924|6|Mentioned|Fig.3|||||||||
25687|Candlow Formation|39943|6|Mentioned|Table 1A|||||||||
25687|Candlow Formation|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25687|Candlow Formation|41975|6|Mentioned|p432|||||||||
25687|Candlow Formation|42199|5|Briefly described|Table 1 P280|||||||||
25687|Candlow Formation|43664|3|Fully described|p31-34|||||||||
25687|Candlow Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.  Includes: White Bull Member, Stockyard Creek Mudstone Member.  Overlies Heliman Formation; Underlies Langdon River Mudstone.||||||07-NOV-08
25687|Candlow Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||19-AUG-04
25687|Candlow Formation|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Etheridge Group. Overlies: Heliman Formation.  Underlies: Langdon River Mudstone.||||||07-NOV-08
25687|Candlow Formation|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Etheridge Group.  Carbonaceous mudstone, fine lithic sandstone, siliceous and siltstone, shale.||||||
25687|Candlow Formation|65887|6|Mentioned|p45 Tb.2|||Sm-Nd isotopic data and depleted mantle model age.||||||
25687|Candlow Formation|66800|6|Mentioned|p926 Table 1.|||||||Overlies Heliman Formation. Is overlain by Langdon River Mudstone.||
25687|Candlow Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||Upper Etheridge Group.|Stockyard Creek Mudstone Member, White Bull Member.|||
25687|Candlow Formation|67341|5|Briefly described|vi|||Forsayth Subprovince, Etheridge Province.|||Stockyard Creek Mudstone Member.|Overlies Heliman Formation. Is overlain by Langdon River Mudstone.||
25687|Candlow Formation|67430|6|Mentioned|p25|||||||||
25687|Candlow Formation|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Five sub-units are mapped separately, two of which are named Members. Age min: Mesoproterozoic?||Unit in Etheridge Group.|Includes White Bull Member and Stockyard Creek Mudstone Member.|Conformably overlies Heliman Formation. Is overlain conformably by Langdon River Mudstone.|Mainly mudstone.|12-MAY-15
25687|Candlow Formation|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Five sub-units are mapped separately, two of which are named Members. Age min: Mesoproterozoic?||Unit in Etheridge Group.|Includes White Bull Member and Stockyard Creek Mudstone Member.|Conformably overlies Heliman Formation. Is overlain conformably by Langdon River Mudstone.|Mainly mudstone.|12-MAY-15
25687|Candlow Formation|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Moderately magnetic. Min Age: Mesoproterozoic?||Unit in Etheridge Group.|Includes White Bull Member and Stockyard Creek Mudstone Member.|Conformably overlies Heliman Formation. Is overlain conformably by Langdon River Mudstone.|Mainly mudstone.|18-MAY-15
25687|Candlow Formation|68355|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Three sub-units are mapped separately, one of which is a named Member. Age min: Mesoproterozoic?||Unit in Etheridge Group.|Includes Stockyard Creek Mudstone Member.|Is overlain conformably by Langdon River Mudstone.|Two units of mudstone, siltstone and mudclast sandstone, commonly carbonaceous and pyritic, locally calcareous, minor quartzose siltstone to sandstone; separated by the Stockyard Creek Mudstone Member.|04-JUN-15
25687|Candlow Formation|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Comprises 5 units of which 3 are unnamed. Age constrained by constituents which are shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Etheridge Group.|Includes Stockyard Creek Mudstone Member, White Bull Member.|Conformably overlain by the Langdon River Mudstone. Conformably underlain by the Heliman Formation.|Mainly mudstones, siltstones and mudclast sandstones.|
25687|Candlow Formation|69591|4|Described|p61-62, p65-66, p68, p82-83|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Similar lithologies, but differing proportions, to Heliman Formation. Their combined thickness is 2000-6000m.||Etheridge Group.|Stockyard Creek Mudstone Member.|Is intruded by the Forest Home Trondhjemite.|Siltstone (with local pseudomorphs after gypsum), carbonaceous mudstone, siliceous siltstone, fine sandstone (characterised by high proportion of sand-sized carbonaceous mudstone clasts); rare thin limestones. Rare stromatolites near top.|
69324|Cannibal Creek Suite|60425|5|Briefly described|p274-5 Appdx. 1|Early Permian|Early Permian|Of Whypalla Supersuite. Contains the Cannibal Creek Granite. S-type. Age: 270Ma and 275Ma (Rb-Sr).||||||07-FEB-11
69324|Cannibal Creek Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Cannibal Creek Granite.|||
79607|Canobie Sequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p21|||Younger than Soldiers Cap Group. Canobie Domain, Mount Isa Inlier; possibly present over much of Soldiers Cap Domain. Deformed with low grade metamorphism, presumably in late Isan Orogeny. Appears as Canobie Succession in the Mount Isa Block Time-Space Plot.|1592 +/- 5 Ma (MDA: Carson et al., in prep.).|||May correlate with Langlovale Group.|Fine-grained, laminated to medium-bedded metasandstone or siltstone, with a schistose foliation.|
79607|Canobie Sequence|69056|5|Briefly described|p56, Time-Space plot sheet|Calymmian|Calymmian|Donors Hill Domain; may extend over a significant part of Soldiers Cap Domain. Intersected in drillhole GSQ Dobbyn 1. Detrital zircon maximum depositional age. Younger than Soldiers Cap Group.
|1592 +/- 5 Ma (Carson et al., 2011).||||Metasandstone or siltstone (with a schistose texture).|16-JAN-17
79607|Canobie Sequence|69591|5|Briefly described|p48|||Canobie Domain. Intersected at the base of GSQ Dobbyn 1. Probably formed during the late phases of the Isan Orogeny. Of unknown distribution.|1592 +/- 5 Ma (maximum depositional age).|||May correlate with the Langlovale Group (Georgetown Inlier).|Fine, laminated to medium-bedded metasandstone or siltstone, with a schistose foliation.|
33429|Canoe Creek Granite|23799|3|Fully described|p97, p11 Tb. 1|Late Triassic|Late Triassic|Previously mapped as part of Wigton Adamellite (Murphy and others, 1976).  Intrudes the Arabanga Volcanic Group.  Of the South-east Queensland Volcanic and Plutonic Intrusives.||||||
33429|Canoe Creek Granite|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
33429|Canoe Creek Granite|60371|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Biotite-hornblende granite to granodiorite.||||||
33429|Canoe Creek Granite|68679|5|Briefly described|p428-429|Late Triassic|Late Triassic|Northern New England Orogen. Parts of this unit were originally mapped as Wigton Granite.||||Intrudes the Aranbanga Volcanic Group.|Fine- to medium-grained, sparsely porphyritic biotite-hornblende granite to granodiorite with small plagioclase and K-feldspar phenocrysts in a granophyric groundmass with coarse accessory sphene. Calc-alkaline, high-K, peraluminous S-type.|
28213|Canyon Dacite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Thickness: 670m. Geological Province: Georgetown Region.||||||25-JUN-15
28213|Canyon Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V26. Assumed to be I-Type.||||||
28213|Canyon Dacite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28213|Canyon Dacite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
28213|Canyon Dacite|43740|5|Briefly described|p13|||||||||
28213|Canyon Dacite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Of the Newcastle Range Volcanic Group).||||||
28213|Canyon Dacite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
28213|Canyon Dacite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|||Grey to brown or purple, sparsely to abundantly porphyritic dacite and crystal-poor to -rich dacitic ignimbrite.|
28213|Canyon Dacite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|||Grey to brown or purple, sparsely to abundantly porphyritic dacite and crystal-poor to -rich dacitic ignimbrite; lesser grey, green or brown rhyolitic volcanic lutite to crystal-rich volcanic arenite to very coarse volcanic rudite.|
36763|Cape Bowen Granite|23423|5|Briefly described|p310 table 7.4||Early Permian|I-type granite.  Of the Cape Melville Supersuite||||||
36763|Cape Bowen Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Cape Bowen Suite.||||
80894|Cape Bowen Suite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |||Cape Bowen Granite.|||
27126|Cape Grenville Volcanics|23420|5|Briefly described|p 146 table 4.5|Early Permian|Late Carboniferous|Also see p 129. In the Janet Ranges Volcanic Group. I-type characteristics. Intruded by Weymouth Granite.||||||
27126|Cape Grenville Volcanics|23431|6|Mentioned|p535|||||||||
27126|Cape Grenville Volcanics|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
27126|Cape Grenville Volcanics|32528|5|Briefly described|Table 2|||||||||
27126|Cape Grenville Volcanics|32706|4|Described|Table 1|||||||||
27126|Cape Grenville Volcanics|33880|6|Mentioned|Map legend|Early Permian|Early Carboniferous|Lower Carboniferous - Lower Permian||||||
27126|Cape Grenville Volcanics|33884|6|Mentioned|Map legend|Early Permian|Carboniferous|Carboniferous to Early Permian||||||
27126|Cape Grenville Volcanics|34581|2|Defined|p140|Permian|Carboniferous|Carboniferous - Permian||||||
27126|Cape Grenville Volcanics|37613|6|Mentioned|p247|||See also Fig.2||||||
27126|Cape Grenville Volcanics|39252|6|Mentioned|Fig.11|||||||||
27126|Cape Grenville Volcanics|39445|5|Briefly described|Table 7|||||||||
27126|Cape Grenville Volcanics|42547|5|Briefly described|p74|||||||||
27126|Cape Grenville Volcanics|43567|5|Briefly described|p402|||||||||
27126|Cape Grenville Volcanics|45076|3|Fully described|p111|||Late Palaeozoic P17.||||||
27126|Cape Grenville Volcanics|71792|5|Briefly described|p33|Early Permian|Late Carboniferous|Northern Coen Inlier.|||||Volcanic breccia, tuff, welded tuff, rhyolite.|
30183|Cape Melville Granite|23423|5|Briefly described|p310 table 7.4||Early Permian|Age: 280+/-2 Ma (Rb-Sr). I-Type granite. Of Cape Melville Supersuite.||||||
30183|Cape Melville Granite|23430|5|Briefly described|p490|||||||||
30183|Cape Melville Granite|23512|5|Briefly described|Map Legend||Early Permian|Of Cape Melville Supersuite.||||||03-JUN-09
30183|Cape Melville Granite|43111|2|Defined|p3|Early Permian||Rb-Sr rock-biotite ages of 281+/-2Ma & 279+/-2Ma.||||||
30183|Cape Melville Granite|60425|5|Briefly described|p54 Tb. 4, p87, p272-3 Appdx. 1|Early Permian|Early Permian|Of Cape Melville Suite (Cape Melville Supersuite). Age: 279+/-2Ma, 280+/-2Ma (Rb-Sr) - more age details p89. Intruded Hodgkinson Formation. I-type. Med.- to coarse-gr., seriate to mod'ly porphyritic (hornblende-) biotite granite - more lith dteails p273.||||||07-FEB-11
30183|Cape Melville Granite|69593|5|Briefly described|p480, p482 Fig.6.6, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated. |279 +/- 2 Ma.|Cape Melville Suite.|||I-type.|
69231|Cape Melville Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Cape Melville Supersuite. Contains Cape Melville Granite. Age: 279+/-2Ma, 280+/-2Ma (Rb-Sr). I-type.||||||07-FEB-11
69231|Cape Melville Suite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |||Cape Melville Granite.|||
30146|Cape Melville Supersuite|23423|3|Fully described|p251||Early Permian|I-type granite. Intrudes Hodgkinson Formation. Units previously mapped as Altanmoui Granite. Also see p310 table 7.4.||||||
30146|Cape Melville Supersuite|23430|5|Briefly described|p493|||I-Type Granites, Daintree Subprovince. Kennedy Province.||||||
30146|Cape Melville Supersuite|23512|5|Briefly described|Map Legend||Early Permian|||||||
30146|Cape Melville Supersuite|43098|6|Mentioned|p35|||||||||
30146|Cape Melville Supersuite|43111|6|Mentioned|p39|||||||||
30146|Cape Melville Supersuite|60425|3|Fully described|p54 Tb. 4, p87-89, p272-5 Appdx. 1|Early Permian|Early Permian|Comprises Altanmoui, Cape Melville, Cape Bowen and Saint Pauls Hill Suites. Age: 280+/-2Ma. Intruded Hodgkinson Formation. I-type, (hornblende-) biotite granites - detailed lithology included.||||||07-FEB-11
30146|Cape Melville Supersuite|63140|6|Mentioned|p581.|||To the NE of Hodgkinson Province.|||||I-type granites.|
30146|Cape Melville Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Brodies Camp, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
30146|Cape Melville Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|280 +/- 2 Ma (Rb/Sr isochron age).||||I-type granitoids.|
30146|Cape Melville Supersuite|69593|5|Briefly described|p478, p480, p482-483, p511|||Daintree Subprovince, Kennedy Igneous Association. Crops out over ~156 km2 in the Melville Range and part of the Altanmoui Range, northern Hodgkinson Province.|? ~280 Ma.||Altanmoui, Cape Bowen, Cape Melville, Saint Pauls Hill Suites.||I-type. (Hornblende-) biotite granite. Granitoids may contain angular quartz fragments and/or high-grade metasedimentary rocks including  gneiss and garnet xenocrysts.|
27361|Cape River Metamorphics|22533|6|Mentioned|p47||Proterozoic|||||||
27361|Cape River Metamorphics|22543|6|Mentioned|p62|Cambrian|Neoproterozoic|Assigned to Cape River Province.||||||17-JAN-07
27361|Cape River Metamorphics|22557|5|Briefly described|p568,9|Proterozoic|Early Paleozoic|||||||07-NOV-08
27361|Cape River Metamorphics|22630|3|Fully described|p 13|Neoproterozoic|Mesoproterozoic|Formerly Cape River beds.||||||17-JAN-07
27361|Cape River Metamorphics|22675|5|Briefly described|p13|||Formerly Cape River Beds.||||||17-JAN-07
27361|Cape River Metamorphics|22844|1|Redefined|p4,6,9,12-41,44-52|Cambrian|Mesoproterozoic|||||||
27361|Cape River Metamorphics|22847|5|Briefly described|p 7||Neoproterozoic|||||||
27361|Cape River Metamorphics|23032|4|Described|p15|||Minimum age may be Stenian.||||||17-JAN-07
27361|Cape River Metamorphics|23049|5|Briefly described|p24|Proterozoic|Proterozoic|||||||
27361|Cape River Metamorphics|23291|6|Mentioned|p28|||Geological Province: Cape River.||||||08-JUL-15
27361|Cape River Metamorphics|23422|3|Fully described|p166, p207 Table 6.3|Early Cambrian|Neoproterozoic|Previously Cape River beds. Geological Province: Cape River Province.||||||
27361|Cape River Metamorphics|23423|6|Mentioned|p267|||||||||
27361|Cape River Metamorphics|23430|4|Described|p459, 461-462|||Cape River Province.||||||
27361|Cape River Metamorphics|23431|5|Briefly described|p537|||Cape River Province.||||||
27361|Cape River Metamorphics|23499|5|Briefly described|map legend|Cambrian|Neoproterozoic|||||||
27361|Cape River Metamorphics|23508|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|||||||
27361|Cape River Metamorphics|23854|6|Mentioned|p858 Fig 1|||||||||
27361|Cape River Metamorphics|23893|6|Mentioned|p7|||Geological Province: Cape River Province.||||||
27361|Cape River Metamorphics|24577|6|Mentioned|p755 Fig. 2|Early Paleozoic|Proterozoic|||||||07-NOV-08
27361|Cape River Metamorphics|37570|6|Mentioned|p123|||||||||
27361|Cape River Metamorphics|39689|6|Mentioned|p49|||||||||
27361|Cape River Metamorphics|40746|4|Described|p345|||||||||
27361|Cape River Metamorphics|40787|5|Briefly described|p321|||Mention Fig.2||||||
27361|Cape River Metamorphics|41260|6|Mentioned|p178|||See also Fig.74||||||
27361|Cape River Metamorphics|41668|5|Briefly described|p6|||||||||
27361|Cape River Metamorphics|41774|6|Mentioned|p29|||||||||
27361|Cape River Metamorphics|42279|6|Mentioned|p27|||||||||
27361|Cape River Metamorphics|42692|5|Briefly described|map legend|Proterozoic||||||||
27361|Cape River Metamorphics|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
27361|Cape River Metamorphics|42747|5|Briefly described|p34|||||||||
27361|Cape River Metamorphics|43213|5|Briefly described|p8, p52-53|||Lolworth-Ravenswood Province. Potential equivalent of Anakie Metamorphic Group farther south. Age from a "possible isochron".|500 +/- 25 Ma.||||Metapelites, quartz-rich metapsammites and amphibolites with tholeiitic and alkaline basalt affinities.|
27361|Cape River Metamorphics|43286|5|Briefly described|Map Legend||Proterozoic|||||||
27361|Cape River Metamorphics|43391|5|Briefly described|Map legend|Ordovician|Cambrian|Geological Province: Lolworth-Ravenswood Block.  Micaceous schist and quartzite.||||||23-JUN-04
27361|Cape River Metamorphics|43480|3|Fully described|1-47|||Previously described as Cape River beds. U-Pb age: 1120Ma.||||||17-JAN-07
27361|Cape River Metamorphics|43603|5|Briefly described|p8||Proterozoic|||||||
27361|Cape River Metamorphics|43706|5|Briefly described|p14|||||||||
27361|Cape River Metamorphics|44207|14|Not recorded|p115|||||||||
27361|Cape River Metamorphics|44699|14|Not recorded|p108|||Previously regarded as Precambrian, probably Silurian or Devonian equated with volcanics and sediments of Windsor Range Volcanics and Bletchington Park Beds.||||||
27361|Cape River Metamorphics|48903|6|Mentioned|p7|||Renamed Cape River Beds.||||||17-JAN-07
27361|Cape River Metamorphics|48908|6|Mentioned|p38||Precambrian|||||||
27361|Cape River Metamorphics|48995|6|Mentioned|p72|||See also Fig.12||||||
27361|Cape River Metamorphics|60425|6|Mentioned|p115|||In western part of Charters Towers region - contain abundant quartzite.||||||07-FEB-11
27361|Cape River Metamorphics|61211|5|Briefly described|p261|Neoproterozoic|Paleoproterozoic|Multiply deformed greenschist to amphibolite grade rocks - gneiss, schist, quartzite, graphitic slate, calc-silicate rocks and amphibolite; high-grade paragneiss present. Intruded by granites of Fat Hen Creek Complex. Geol. Prov: northern Tasminides (Qld)||||||07-NOV-08
27361|Cape River Metamorphics|62074|5|Briefly described|p1-2|Early Cambrian|Neoproterozoic|Basement in Lolworth-Ravenswood Block. Multiply deformed; underwent high T/low P metamorphism in early to middle Ordovician.||||||
27361|Cape River Metamorphics|62075|6|Mentioned|p9 Fig.2|Early Cambrian|Neoproterozoic|Unit in the Ravenswood Batholith.||||||
27361|Cape River Metamorphics|63154|5|Briefly described|p285 Fig. 5|Cambrian|Early Cambrian|Geological province: Charters Towers Province.||||||
27361|Cape River Metamorphics|63562|6|Mentioned|p342|Mesoproterozoic|Mesoproterozoic|Western Lolworth-Ravenswood Block, North Qld. Discussed and discounted as probable source for Heavitree Quartzite.|1.25-1.10 Ga.|||||
27361|Cape River Metamorphics|64707|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic III|Biotite gneiss, mica schist, quartzite and amphibolite; local migmatite and leucogranite veins.||||||
27361|Cape River Metamorphics|65380|6|Mentioned|p679, p677 Fig.9|||||||||
27361|Cape River Metamorphics|65706|4|Described|p9 Fig.3, p10, p13 Tb.1, p23, p42 Fig.10|Early Cambrian|Neoproterozoic|Forms basement to the Thalanga Province. Appears as Cape River beds on p134.||||Intruded and metamorphosed by Ravenswood Granodiorite Complex; unconformably underlies Bulgonunna Volcanic Group.|Siltstone, mudstone, sandstone, acid tuff, phyllite, schist, gneiss, amphibolite, marble.|
27361|Cape River Metamorphics|67455|5|Briefly described|p574 Fig.1, p583, pp590-591.|Lower Paleozoic|Lower Paleozoic|Charters Towers Province. 100 km south of Greenvale Province. Has low-angle, intense foliation (S2) and recumbent folds, inferred to have formed in an extensional tectonic setting.||||||
27361|Cape River Metamorphics|67848|5|Briefly described|p16.|||Charters Towers Province. Inversion and folding occurred in the Silurian, correlating with younger phases of the Benambran Orogeny.||||||
27361|Cape River Metamorphics|68338|5|Briefly described|Map legend.|Cambrian|Neoproterozoic|Cape River Province. High K, Th and U radiometric responses.|||||Biotite gneiss, mica schist, quartzite and amphibolite; local migmatite and leucogranite veins.|
27361|Cape River Metamorphics|68339|5|Briefly described|Map legend.|Cambrian|Neoproterozoic|Cape River Province.|||||Quartzose arenite, subordinate mudstone.|
27361|Cape River Metamorphics|68340|5|Briefly described|Map legend.|Cambrian|Neoproterozoic|Cape River Province.|||||Quartzose arenite, subordinate mudstone.|
27361|Cape River Metamorphics|68478|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Cape River Province. The 8 facies are mapped separately.|||||Undivided: biotite gneiss, mica schist, quartzite, local amphibolite; grading into migmatite.|
27361|Cape River Metamorphics|68479|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Includes 1 undivided, and 6 separately mapped unnamed units.|||||Undivided: biotite gneiss, mica schist, quartzite, local amphibolite; grading into migmatite.|
27361|Cape River Metamorphics|68553|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|||||||27-JUL-15
27361|Cape River Metamorphics|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
27361|Cape River Metamorphics|68731|5|Briefly described|p132, pp136-141, p145, p147, pp218-221|Lower Ordovician|Neoproterozoic|Charters Towers Province. Previously named and described by Paine, Harding, and Clarke (1971) as the Cape River beds. Age loosely constrained (p139) between <905-483 Ma.|< 905-483 Ma||Includes the Morepork Member.|Intruded by the Cornelia Orthogneiss and the Fat Hen Creek Complex. Correlated with the Charters Towers Metamorphics on lithological grounds.|Comprises dominantly quartzose metasedimentary schist and gneiss derived from sandstone and abundant mudstone.|02-JUL-14
27361|Cape River Metamorphics|68822|6|Mentioned|p320 Fig.3, p323|Cambrian|Cambrian|Rift volcanics. Charters Towers Province.||||||
27361|Cape River Metamorphics|68900|6|Mentioned|p11|||Rocks previously assigned to this unit are now reassigned to the Seventy Mile Range Group. [Replaces the Cape River beds?].||||||
27361|Cape River Metamorphics|69592|5|Briefly described|p280, p292|Paleozoic|Paleozoic|NW Charters Towers Province. Intruded by granitoids of the Lolworth Batholith.||||Is intruded by Upland Supersuite; Amarra, Grasstree and Hodgon Suites.|Middle to upper amphibolite facies metamorphic rocks including migmatites in places.|
27361|Cape River Metamorphics|69599|6|Mentioned|p644|||In the Charters Towers region, this unit is intruded by 27-25 Ma volcanic plugs.||||||
27361|Cape River Metamorphics|69952|6|Mentioned|p61|||Close similarities with Oasis Metamorphics led to this latter unit being separated (Withnall et al., 2002) from Einasleigh Metamorphics.||||||
27361|Cape River Metamorphics|70740|6|Mentioned|p37|||||||||
27361|Cape River Metamorphics|70744|5|Briefly described|p939-941, p947|Neoproterozoic|Neoproterozoic|Charters Towers Province. Possibly equivalent to lower Argentine Metamorphics. Contains abundant "Grenville-age" detrital zircons (1.3 - 1 Ga). 39Ar/40Ar cooling ages by Fergusson et al. (2005). Intruded by Ravenswood Batholith plutons aged 510-460 Ma.|c.445-410 Ma (estimated from Fig.7).||||Contains abundant thick metasedimentary quartzose psammitic gneisses.|
27361|Cape River Metamorphics|70749|5|Briefly described|p42-44, p49, p52-53, p55|Cambrian|Neoproterozoic|Charters Towers Province. Characterised by abundant 1300-900 Ma (late Mesoproterozoic = Grenvillian) aged detrital zircons, and maximum depositional age of ~580 Ma or older. Zircons sourced from Musgrave Province.|~900 Ma (maximum depositional age).|||||
27361|Cape River Metamorphics|70838|6|Mentioned|p276|Ediacaran|Ediacaran|Charters Towers Province.||||||
27361|Cape River Metamorphics|70839|5|Briefly described|p342-343|Late Neoproterozoic|Late Neoproterozoic|Geological province: Charters Towers Province. Age inferred by Fergusson et al., 2007.||||||
27361|Cape River Metamorphics|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Charters Towers Province, Thomson Orogen. ||||||
27361|Cape River Metamorphics|72088|6|Mentioned|p9|||Charters Towers Province. Formerly the Cape River beds.|||||Meta-sedimentary rocks.|
27361|Cape River Metamorphics|73425|5|Briefly described|p2, 15-16, 18|Neoproterozoic|Neoproterozoic|Fergusson et al. (2007). Charters Towers Province, northeast Thomson Orogen.||||Is intruded by Fat Hen Creek Complex.||
27361|Cape River Metamorphics|73472|6|Mentioned|p114, p116|Neoproterozoic|Neoproterozoic|Crystalline basement rocks exposed within Porcupine Gorge.||||Unconformably overlain by Boonderoo beds (angular unconformity).||
27361|Cape River Metamorphics|73600|6|Mentioned|p202|||||||||
81003|Cape Upstart Granite|68679|6|Mentioned|p363|Early Cretaceous|Early Cretaceous|||||||
81003|Cape Upstart Granite|69594|5|Briefly described|p567, p569, p571 Fig.7.47|Early Cretaceous|Early Cretaceous|Bowen-Mackay region. Geochemical plots.|103.3 +/- 1.1 Ma (K-Ar biotite: Allen et al. 1998)||||Dominantly biotite leucogranite. Miarolitic cavities, pegmatitic patches and microgranophyric textures. Mafic enclaves scarce or absent. Closely associated with gabbro, diorite and rare granodiorite.|
36519|Cape Woora granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 169.||||||
32037|Capella Creek Group|22482|4|Described|p487, Fig.1||Middle Devonian|Formerly Capella Creek beds.||||||24-NOV-08
32037|Capella Creek Group|23077|5|Briefly described|p716|||||||||
32037|Capella Creek Group|23468|6|Mentioned|Table 1 p 296|||||||||
32037|Capella Creek Group|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
32037|Capella Creek Group|24399|5|Briefly described|p271, p277|Middle Devonian|Early Devonian|Rhyolite volcanics.  Geological Province: New England Fold Belt.  See also p279 Fig. 4.||||||
32037|Capella Creek Group|24491|3|Fully described|p15|Middle Devonian|Silurian|Supersedes Capella Creek beds and Capella Creek Formation. Includes Mount Dick beds, Mount Warner Volcanics and Raspberry Creek Formation.||||||
32037|Capella Creek Group|50208|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Raspberry Creek Formation, Mount Warner Volcanics, Mount Dick beds.||||||
32037|Capella Creek Group|50317|5|Briefly described|Map Legend|Devonian|Devonian|Includes the Raspberry Creek Formation and Mount Warner Volcanics.||||||09-JUN-04
32037|Capella Creek Group|60557|5|Briefly described|p22|Middle Devonian|Middle Devonian|Includes the Raspberry Creek Formation.||||||09-JUN-05
32037|Capella Creek Group|61147|5|Briefly described|pp376-379. |Middle Devonian|Middle Devonian|Kirkegaard et al. (1970) included within this unit a suite of rocks formerly called Moongan Rhyolite (Hawkins 1962).|||Includes Mount Dick beds, Mount Warner Volcanics and Raspberry Creek Formation.|Includes the Mount Dick beds, Mount Warner Volcanics and Raspberry Creek Formation. Intruded by the Mount Morgan trondhjemite and the Bouldercombe Complex.|Predominantly andesitic to dacitic extrusive and volcaniclastic rocks; overlain by acid and andesitic lavas and volcanolithic sediments, including minor limestones; and an upper, predominantly andesitic sequence with minor limestones.|
32037|Capella Creek Group|61392|5|Briefly described|p165 Fig. 2|Givetian|Pridoli|Part of the 'Calliope Volcanic Assemblage' (Morand 1993). More recently referred to as the 'Mount Morgan Stratigraphic Assemblage' (Barker et al 1997).||||||07-FEB-11
32037|Capella Creek Group|61730|5|Briefly described|p994 Fig.1|Middle Devonian|Late Silurian|Includes Mount Warner Volcanics, Mount Dick beds. Geological Province: Yarrol Province. See also p1000.||||||
32037|Capella Creek Group|61808|5|Briefly described|p445, p446, p447 Fig. 1|Middle Devonian|Early Devonian|Subdivided into Mount Dick beds, Mount Warner Volcanics and Raspberry Creek beds by GSQ and other workers. QLD. Comprises jaspers, manganiferous jaspers and cherts. Associated with VHMS deposits.||||||
32037|Capella Creek Group|63600|5|Briefly described|p900 Fig. 1, p915|Middle Devonian|Middle Devonian|Includes Mount Warner Volcanics. See also p917-918.||||||07-FEB-11
32037|Capella Creek Group|68008|3|Fully described|p1, p17, p22, p26-42, p48, p61, p67, p69|Middle Devonian|Middle Devonian|See also p71, p89, p308-309, p317-318, p353, p359, p361, p395-396, p478-479, p487-490, p568, p576-579, p621-623. Originally Capella Creek beds of Kirkegaard et al. (1970). Subdivided by Taube (1986) who named the lower silicic section the Mount Warner Volcanics. Both were included in the Capella Creek Formation (Morand (1993), which was later subdivided by Messenger and Taube (1994) into three units: basal Mount Dick beds, Mount Warner Volcanics and topmost Capella Creek beds. These were combined as the Capella Creek Group by the Yarrol Project Team (1997), who renamed the Capella Creek beds as the Raspberry Creek Formation. Hosts the Mount Morgan Au-Cu orebody. Similar geochemistry to Mount Morgan Trondhjemite. Structure discussed. Geophysics modelling.|||Mount Dick beds, Mount Warner Volcanics, Raspberry Creek Formation, Ginger Creek beds.|Is overlain unconformably by Mount Hoopbound and Balaclava Formations. Is intruded by Mount Morgan Trondhjemite, Bundaleer Tonalite, and Gavial and Quarry Gabbros. May correlate with Craigilee beds.|Contains a belt of volcanic and plutonic rocks.|
32037|Capella Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Erebus, Marble Waterhole, Craigilee, Calliope, Munbooree and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
32037|Capella Creek Group|68679|5|Briefly described|p311-314, p316, p338, p401, p426, p467|Devonian|Late Silurian|Originally the Capella Creek beds (Kirkegaard, Shaw and Murray, 1970). The lower part was separated as the Mount Warner Volcanics by Taube (1986). The two parts were reunited as the Capella Creek Formation by Morand (1993). Undeterred, Messenger and Taube (1994) named the basal Mount Dick beds and the overlying Mount Warner Volcanics [again], but retained Capella Creek beds [sic] for the more mafic upper part. Murray et al. (2012) upgraded Messenger and Taube's (1994) scheme to Group status and renamed the mafic upper part the Raspberry Creek Formation. Has volcanic and plutonic geochemistry similar to that of modern island arcs.|||Mount Dick beds, Mount Warner Volcanics, Raspberry Creek Formation.|Is faulted against the Mount Alma Formation. Is intruded by the Mount Morgan Trondhjemite, Gavial, Quarry Gabbros and Bundaleer Tonalite.||
29741|Capsize Creek Complex|22845|6|Mentioned|Fig6|Permian|Carboniferous|||||||
29741|Capsize Creek Complex|22846|2|Defined|p6,7,12,20-4,41,75|Early Permian|Silesian|Contains Yabba Creek, Claddagh and Gallangowan Granodiorites.||||||
29741|Capsize Creek Complex|23609|4|Described|p6-7, 9, 11|||Also see Fig 1 p6. North D'Aguilar Block.||||||
29741|Capsize Creek Complex|44923|5|Briefly described|Map Legend||Permian|||||||
29741|Capsize Creek Complex|50320|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
29741|Capsize Creek Complex|60370|5|Briefly described|Map Legend|Permian|Carboniferous|Geological Province: North D'Aguilar Subprovince. Biotite granodiorite; biotite-hornblende granodiorite; biotite-hornblende quartz diorite; porphyritic biotite-hornblende quartz microdiorite.||||||02-SEP-04
29741|Capsize Creek Complex|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Claddagh, Coppermine Creek, Gallangowan, Karandah and Yabba Creek Granodiorites, are all mapped under the same symbol, Cgd.||||||
29741|Capsize Creek Complex|68679|5|Briefly described|p325, p404, p470|Late Carboniferous|Late Carboniferous|Kilkivan-Manumbar area, North D'Aguilar Subprovince. Syntectonic granitoids.||||||
29741|Capsize Creek Complex|69056|6|Mentioned|p57|||Stated to be the previous name for the Dipvale Granodiorite.||||||
70427|Captain Osborne Granite|68679|5|Briefly described|p410, p421-422|||Gayndah-Gladstone belt, southern part of the northern New England Orogen.|259.8 +/- 2.1 Ma (U-Pb zircon: Black, unpub.).||||Coarse-grained, equigranular to porphyritic hornblende-biotite monzogranite.|
68158|Caramar Siltstone|60281|5|Briefly described|Fig. 33 Appendix 1|Cretaceous|Cretaceous|Of the Maryborough Formation.  Underlies the Burrum Coal Measures.  Geological Province: Maryborough Basin.||||||27-APR-05
23469|Carbethon Gabbro|23052|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
23469|Carbethon Gabbro|23161|4|Described|p48 table6||Early Cretaceous|||||||
23469|Carbethon Gabbro|42701|2|Defined|p102|Early Cretaceous||Age assumed||||||
23469|Carbethon Gabbro|44245|5|Briefly described|Map Legend||Cretaceous|||||||
36108|Cardross Orthogneiss|23291|4|Described|p87 Tb. 3.6p|Paleoproterozoic|Paleoproterozoic|Parent: Dargalong Metamorphic Group. Age: 1580Ma (U-Pb zircon SHRIMP). Geological Province: Georgetown Region.||||||01-APR-15
36108|Cardross Orthogneiss|23500|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: ~ 1580 Ma, SHRIMP||||||
36108|Cardross Orthogneiss|24485|5|Briefly described|p22, 26|Mesoproterozoic|Mesoproterozoic|Age: ~1585-1580Ma. Parent: Dargalong Metamorphic Group||||||
36108|Cardross Orthogneiss|24486|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Dargalong Metamorphics. Geological Province: Yambo Sub-province (Etheridge Province).||||||01-APR-15
36108|Cardross Orthogneiss|68337|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Dargalong Metamorphics.|||Pale grey to grey, foliated, fine- to medium-grained, uneven-grained to porphyritic biotite granite to granodiorite, gneissic (muscovite)-biotite granite, granitic gneiss.|
36108|Cardross Orthogneiss|69591|5|Briefly described|p70|||The augen gneiss within the Dargalong Metamorphics. It is geochemically similar to I-type granodiorite. Comparable in age to the Arkara Gneiss in the Coen Inlier. Underwent metamorphism c.1575 Ma (Blewett et al., 1998).|c.1585 Ma (emplacement).||||Augen gneiss within the Dargalong Metamorphics.|
36436|Cardwell Supersuite|23617|5|Briefly described|p55|||||||||
28102|Carew Greenstone|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
28102|Carew Greenstone|22781|4|Described|p21|Proterozoic|Proterozoic|Holroyd Group||||||
28102|Carew Greenstone|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group, Coen Inlier.||||||
28102|Carew Greenstone|23431|5|Briefly described|p535|||||||||
28102|Carew Greenstone|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group.||||||
28102|Carew Greenstone|43596|4|Described|p19 Tb. 1, p22|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group. Comprises a number of mafic sills up to 1500m thick. Subdivided into variants which may have equivalents in Edward River Metamorphic Group. Intrudes Astrea Fm, Sugarbag Ck.Quartzite. Metadolerite, etc - detailed description p19 and p22.||||||07-APR-15
28102|Carew Greenstone|43738|6|Mentioned|p48|||||||||
28102|Carew Greenstone|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||24-JAN-05
28102|Carew Greenstone|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. 500-1000m thick. Occurs between Edward River and Ethel Creek. Transgressive sills intrude lower part of Holroyd Group. Tholeiitic chemistry indicates mantle derivation of hot magma.||Holroyd Group.|||Metadolerite, tremolite-actinolite amphibolite, chlorite-tremolite-sericite-talc rock.|
31111|Cargoon Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31111|Cargoon Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
31111|Cargoon Granodiorite|43480|2|Defined|7-22|Devonian|Silurian|||||||
31111|Cargoon Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Grey, medium-grained, porphyritic hornblende-biotite granodiorite to tonalite with scattered phenocrysts of plagioclase up to 1.5 cm.|
31111|Cargoon Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Grey, medium-grained, porphyritic hornblende-biotite granodiorite to tonalite with scattered phenocrysts of plagioclase up to 1.5 cm.|
31111|Cargoon Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
69011|Carinya Granite|61087|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Weakly to moderatly folated, fine to coarse-grained, equigranular, leucocratic biotite granite; medium grained, equigranular biotite-hornblende granodiorite to diorite.||||||
69011|Carinya Granite|65388|4|Described|p240-241, 280, p236 Fig. 81, p340|Late Carboniferous|Early Carboniferous|New name. Previously incorporated in undifferentiated Palaeozoic unit. Intrudes Yerilla Metamorphics. May be intruded by the Culcraigie Granite.Typically weakly to moderately foliated, fine to coarse-grained, equigranular, leucocratic biotite granite. Foliation suggests age similar to Donore Granite Gneiss, but geochem. like later Carboniferous granites.||||||
69011|Carinya Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Auburn Subprovince. This unit, as well as the Mount Clairvoyant Granite, Donore Granite Gneiss and Horse Granite Gneiss, are all mapped under the same symbol, Cga.||||||
69011|Carinya Granite|68679|5|Briefly described|p312, p406|Carboniferous|Carboniferous|Northern New England Orogen. Age uncertain.|||||Weakly to moderately foliated, leucocratic biotite granite; biotite-hornblende granodiorite to diorite.|
29202|Carleton Monzogranite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
29202|Carleton Monzogranite|22781|4|Described|p29|Paleozoic|Paleozoic|Flyspeck  Supersuite||||||07-NOV-08
29202|Carleton Monzogranite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite.||||||
29202|Carleton Monzogranite|42610|3|Fully described|p28|Early Devonian|Early Devonian|Age assumed similar to other Flyspeck Supersuite rocks, about 400Ma.||||||
29202|Carleton Monzogranite|43738|6|Mentioned|Fig.12,p38|||||||||
29202|Carleton Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
70386|Carmans Syenogranite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Pale to dark pink, medium-grained, uneven-grained, leucocratic biotite-alkali feldspar granite.|
27363|Carmila beds|23037|4|Described|p12,7,24,5,48-51,5,||Early Permian|Underlying unit Mount Benmore Volcanics.||||||
27363|Carmila beds|23042|3|Fully described|p9,12,21,2,40-53,67|Early Permian|Late Carboniferous|||||||
27363|Carmila beds|23162|5|Briefly described|p883||Early Permian|Age: 294.2+/-2.8Ma - correlate of Lizzie Creek Volcanics, based on fossil assemblage. Of Dumbleton Rocks Ignimbrite.||||||28-MAY-08
27363|Carmila beds|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pc].  Siltstone and mudstone, volcanilithic sandstone and conglomerate and minor altered basalt; local rhyolitic to dacitic ignimbrite and volcaniclastic rocks.||||||
27363|Carmila beds|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27363|Carmila beds|39252|5|Briefly described|p21|||||||||
27363|Carmila beds|39262|6|Mentioned|p130|||||||||
27363|Carmila beds|40623|5|Briefly described|p79|||||||||
27363|Carmila beds|41246|6|Mentioned|Map legend|Permian||||||||
27363|Carmila beds|41576|6|Mentioned|p7|||||||||
27363|Carmila beds|41922|4|Described|Table 1, P8|||||||||
27363|Carmila beds|41923|6|Mentioned|p21|||||||||
27363|Carmila beds|42249|6|Mentioned|Table 1 P22|||||||||
27363|Carmila beds|42281|5|Briefly described|p71|||||||||
27363|Carmila beds|43017|6|Mentioned|p377|||||||||
27363|Carmila beds|50213|5|Briefly described|Map legend|Permian|Permian|Siltstone and mudstone, subordinate volcanilithic sandstone and conglomerate.||||||13-MAY-04
27363|Carmila beds|60282|6|Mentioned|p5|||Geological Province: Bowen Basin.||||||
27363|Carmila beds|60445|5|Briefly described|p5, p45|Permian|Permian|Rhyolitic to dacitic ignimbrites, felsic volcanic rudite, altered basalt, conglomerate, sandstone, siltstone and shale; contains breccia pipes. Conformably overlies Mountain View Volcanics; overlain by Back Creek Group sedimentary rocks. See also p50, p5||||||28-MAY-08
27363|Carmila beds|60473|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Volcanolithic conglomerate and sandstone; feldspathic sandstone and interbedded rhyolitic to dacitic volcanic rocks; minor siltstone, mudstone, coal. Rhyolitic to dacitic ignimbrite.||||||17-SEP-04
27363|Carmila beds|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Siltstone, mudstone, volcanolithic sandstone and conglomerate, basalt, rhyoltic to dacitic volcaniclastic rocks.||||||
27363|Carmila beds|60479|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Rhyolitic to dacitic volcaniclastic rocks, basalt, siltstone and mudstone, volcanolithic sandstone and conglomerate.||||||
27363|Carmila beds|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Rhyolitic to dacitic volcaniclastic rocks, basalt, conglomerate. Of the Lizzie Creek Volcanic Group.||||||
27363|Carmila beds|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Rhyolitic to dacitic volcaniclastic rocks, basalt, conglomerate, siltstone and mudstone, sandstone.||||||
27363|Carmila beds|60557|5|Briefly described|p24|||See also Camilla beds.  Represent the Bowen Basin early rift phase.  Comprise siltstone, mudstone, volcaniclastic sandstone and conglomerate, and local altered basalt.Geological Province: Bowen Basin.||||||09-JUN-05
27363|Carmila beds|60787|5|Briefly described|p9|Permian|Permian|||||||
27363|Carmila beds|61035|4|Described|p6, p42, p51, p53, p55, p56, p68|Early Permian|Early Permian|Of the Lizzie Creek Volcanics. Underlain by Mount Buffalo Volcanics. Age: ~294Ma (Allen et al., 1998), broadly synchronous with Camboon Volcanics in the Aurburn Arch. These beds are broadly coeval. Geo Prov: Connors Sudprovince.||||||07-FEB-11
27363|Carmila beds|61777|5|Briefly described|p224, p230|||Geological Province: Yarrol Province.||||||07-FEB-11
27363|Carmila beds|61916|5|Briefly described|Map legend|Early Permian|Early Permian|Sitlstone and mudstone, volcanolithic sandstone and conglomerate; minor altered basalt. Hornfels, silicified mudstone, siltstone, sandstone. Rhyolitic to dacitic ignimbrite with subordinate, poorly sorted, volcanolithic sandstone and conglomerate.||||||
27363|Carmila beds|61917|5|Briefly described|Map legend|Early Permian|Early Permian|Pebble to cobble conglom. and minor sst. Siltstone and mudstone, volcanilithic sst. and conglom. Hornfels, silicified mudstone, siltstone and sst. Rhyolitic to dacitic ignimbrite, volcanilithic sst. and conglom. Hornfels, silicified volcanic rocks.||||||
27363|Carmila beds|65114|5|Briefly described|p383 Tb.1, p395|Cisuralian||ca 297-278 Ma; Tectonic unit: Bowen Basin - Taroom Trough; SHRIMP age  of 294.2 +/- 2.8 Ma (Ignimbrite) and of  305.4 +/- 3.4 Ma  and 292.8 +/- 3.0 Ma (rhyodacitic ignimbrite) - 2 different references for dates||||||
27363|Carmila beds|65388|3|Fully described|p133-145;  p137-138, p31, 32, 34, 48|Early Permian|Early Permian|Of Lizzie Creek Volcanic Group, Connors Arch. Overlies Mountain View Volcanics locally, Mount Benmore Volcanics, Mount Buffalo Volcanics, Langdale Hill Rhyolite probably all unconformably. Overlain by Back Creek Group, Calen Coal Measures. Intruded by Ben Mohr and Mount Bridgeman Complexes and Swayneville Granite. First described Jensen et al 1966. Previous mapping included rocks now assigned to older units eg  Leura Volcanics, Cobweb Mountain Rhyolite, Mount Benmore Volcanics and Broadsound Range Volcanics.  Correlated with Camboon Volcanics, Woolein Formation. SHRIMP Age 294+/-3 Ma. This name no longer used for rocks around Charon Point. Previously included rocks now mapped as Glenprairie beds, Tanderra Volcanics, Wongrabry beds. No one section is typical of the unit. Typical lithofacies include sandstone, conglomerate, rhyolitic ignimbrite and thinly interbedded sandstone and mudstone. See also p58, 59, 60, 64, 68, 70, 75, 84, 85, 86, 90, 123, 132, 174, 233, 358, 362, 393, 437, 441, 443, 447.||||||
27363|Carmila beds|65706|4|Described|p11; Tb.1 p15,16,17,18,19; p32 Fig.6|Early Permian|Early Permian|See also p36-7, p49, p55, p57-62, p99-100, p103, p141. Probably equivalent to parts of the Back Creek Group; possibly equivalent to Airlie volcanics; ?disconformably underlies Calen Coal Measures. Hosts the Silver Wattle Au reef deposit and other gold and Au-Ag-Cu mineralisation; hosts iron (hematite) mineralisation.||Member of the Lizzie Creek Volcanic Group.||Intruded by Urannah Igneous Complex, Hecate Granite, Mount Jukes Syenite Complex. Downfaulted against Edgecumbe beds; probably unconformable on Campwyn Volcanics.|Siltstone and mudstone, volcanolithic sandstone, conglomerate and minor altered basalt, with local acid to intermediate pyroclastics, flows and volcanic rocks.|
27363|Carmila beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Connors Subprovince.||||||
27363|Carmila beds|68679|4|Described|p308, p347, p349, p353, p355, p358-361|Permian|Permian|See also p364, p368, p379, p396. Malone et al. (1969); several re-assignments to other units have been made by various authors and are listed. An extensive unit in Connors Subprovince: outcrop occurrences detailed. The unit's area was restricted to a continuous belt along the eastern flank of the Connors Subprovince by Withnall et al. (2009). Fluvial, fluvio-lacustrine deposits; rocks containing marine fossils are assigned to the Back Creek Group. Some coaly layers have Pennsylvanian-Cisuralian carbonised plant remains (Fig.5.46). Age relationships discussed, particularly with Mount Benmore Volcanics; may be equivalent to Cobweb Mountain Rhyolite, and may correlate with the Woolein Formation and (in part) Mount Buffalo Volcanics.|292.8 +/- 2.9 Ma (Fanning et al., 2009).|Lizzie Creek Volcanic Group.||Overlies Mount Benmore Volcanics, and Langdale Hill Rhyolite unconformably. Is overlain by the Calen Coal Measures. Abuts the Back Creek Group.|Felsic volcanics (welded ignimbrites, lava flows), pebble to boulder conglomerate, conglomeratic sandstone, tuffaceous (feldspathic) sandstone, siltstone, mudstone, shale; minor dacitic to rhyolitic tuff, basalt, andesite; rare volcanic breccia.|
27363|Carmila beds|68901|5|Briefly described|p2, p12, p13, p16|Early Permian|Early Permian|New England Orogen, Bowen Region. SHRIMP date from Withnall et al. (2009).|292.8+/-2.9 Ma SHRIMP on rhyolite sample.|||||26-SEP-18
27363|Carmila beds|69582|5|Briefly described|p45, p57, p60|Early Permian|Early Permian|Forms basement to the Styx Basin. Intersected in GSQ St Lawrence 1.||||Conformably overlain by the Back Creek Group.|Siltstone, mudstone, volcanolithic sandstone, conglomerate, minor altered basalt and local rhyolitic to dacitic volcanic rocks.|
27363|Carmila beds|69952|6|Mentioned|p85|Permian|Permian|New England Orogen.||||||
27363|Carmila beds|70673|6|Mentioned|p9|Permian|Permian|||||||
27363|Carmila beds|71710|5|Briefly described|p368|||Bowen Basin. SHRIMP zircon ages|294.2 +\- 2.8 Ma SHRIMP zircon age|||Age-equivalent correlation to Reids Dome beds (southern Bowen Basin); palynologically correlatable to Aramac Coal Measures (northern Galilee Basin)||
27363|Carmila beds|72297|6|Mentioned|p697|||||||Is overlain by the Calen Coal Measures.||
27363|Carmila beds|73036|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Siltstone + mudstone, volcanilithic sandstone + conglomerate + minor altered basalt; local rhyolitic to dacitic ignimbrite + rhyolitic to andesitic to dacitic volcaniclastic rock (poorly sorted, volcanic sandstone and breccia and ignimbrite).|
78913|Carminya Granodiorite|65388|2|Defined|p361, p135 Fig. 53, p362, 363, 383|Early Permian|Late Carboniferous|Northern Connors Arch, Connors Province. Probably intrudes rocks tentatively assigned to the Leura and Whelan Creek Volcanics. May post-date Strathdee Granodiorite. Age tentative. Mainly grey, pinkish grey, greenish grey, or brown to dark reddish brown (extensively weathered), medium to fine-grained, uneven-grained to slightly porphyritic (titanite-) biotite-hornblende granodiorite.||||||29-APR-16
24212|Carnes Granodiorite|23291|4|Described|p48, p98 Tb 3.11|Permian|Carboniferous|Geological Province: Georgetown Region.||||||25-JUN-15
24212|Carnes Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 16. I-Type.||||||
24212|Carnes Granodiorite|35921|6|Mentioned|p38|||||||||
24212|Carnes Granodiorite|36216|2|Defined|p210|Mesoproterozoic|Mesoproterozoic|||||||
24212|Carnes Granodiorite|36937|6|Mentioned|p229|||||||||
24212|Carnes Granodiorite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
24212|Carnes Granodiorite|40860|4|Described|p112|||||||||
24212|Carnes Granodiorite|43259|4|Described|Appendix 1,p16.||Permian|||||||
24212|Carnes Granodiorite|43664|6|Mentioned|p96||Permian|||||||
24212|Carnes Granodiorite|43740|4|Described|p32||Early Permian|||||||
24212|Carnes Granodiorite|50210|5|Briefly described|Map Legend|Permian|Permian|||||||
24212|Carnes Granodiorite|50595|5|Briefly described|Map Legend|Early Permian|Early Permian|Biotite granodiorite.||||||01-JUL-04
24212|Carnes Granodiorite|68352|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Medium- to coarse-grained biotite granodiorite, with K-feldspar tending to poikilitic.|
24212|Carnes Granodiorite|68415|5|Briefly described|Map Legend|Permian|Permian|Early Permian age. Of the Kennedy Province.|||||Medium to coarse-grained biotite granodiorite.|
24212|Carnes Granodiorite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Western Georgetown region. Unassigned.|||||I-type. Hornblende-biotite and biotite granodiorite (to tonalite), biotite granite; some dolerite.|
37016|Carol Creek Rhyolite|23251|5|Briefly described|Table 1 p8||Late Triassic|Name used interchangeably with Carol Creek Member. No isotopic dating; relationship to other units indicates a late Triassic age. Of South East Queensland Volcanic and Plutonic Province. See Carol Creek Member Table3 p25.||||||21-JUN-06
37016|Carol Creek Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
37016|Carol Creek Rhyolite|44928|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics Group. Rhyolitic tuff (breccia) and rhyolitic tuff.||||||11-MAY-18
37016|Carol Creek Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Upper: crudely bedded, poorly sorted breccia with dacitic or andesitic groundmass. Lower: clastic apron of rhyolite, rhyodacite to dacite, airfall tuffs, pyroclastic flows, epiclastic mudstone and rare sandstone. More details in text.|
37016|Carol Creek Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
26462|Carolina Sandstone Member|22538|6|Mentioned|Fig3 P709|||||||||
26462|Carolina Sandstone Member|23395|6|Mentioned|p385|||||||||
26462|Carolina Sandstone Member|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26462|Carolina Sandstone Member|31348|6|Mentioned|p344|||||||||
26462|Carolina Sandstone Member|35114|6|Mentioned|Table.1|||||||||
26462|Carolina Sandstone Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26462|Carolina Sandstone Member|36012|3|Fully described|Table 2|||||||||
26462|Carolina Sandstone Member|38557|5|Briefly described|p293|||||||||
26462|Carolina Sandstone Member|38584|4|Described|p13|||||||||
26462|Carolina Sandstone Member|40691|6|Mentioned|Fig.4|||||||||
26462|Carolina Sandstone Member|41721|4|Described|p18|||Of the Seigal Volcanics. Thickness: 20m. Flaggy to massive, fine-grained, dark red weathering grey sandstone with some siltstone interbeds.||||||02-AUG-07
26462|Carolina Sandstone Member|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26462|Carolina Sandstone Member|42385|6|Mentioned|Fig.5 P8|||||||||
26462|Carolina Sandstone Member|42812|5|Briefly described|p11|||Of Seigal Volcanics.||||||03-AUG-06
26462|Carolina Sandstone Member|43036|6|Mentioned|Fig.5|||||||||
26462|Carolina Sandstone Member|44305|14|Not recorded|p.11||Neoproterozoic|Defn. on Tech.File E/53-8. opp.p.6. U.Prot||||||
26462|Carolina Sandstone Member|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26462|Carolina Sandstone Member|45162|6|Mentioned|p14|||See also Fig.4||||||
26462|Carolina Sandstone Member|49001|5|Briefly described|p5|||Previously defined as a member of the Peters Creek Volcanics. See also p71||||||03-AUG-06
26462|Carolina Sandstone Member|60483|5|Briefly described|p7 Fig. 5|||Of Seigal Volcanics (Tawallah Group). Geological Province: McArthur Basin.||||||05-OCT-07
26462|Carolina Sandstone Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Seigal Volcanics.||||||03-JUN-09
26462|Carolina Sandstone Member|63112|6|Mentioned|p1192 Tb.1|||<20 m thick. Separates two dolerite sills.||Unit in Seigal Volcanics.|||Fine-grained sandstone.|
26462|Carolina Sandstone Member|64817|6|Mentioned|p353 Fig.4 |||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|65228|6|Mentioned|Fig.02.|||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|65340|6|Mentioned|p12 Fig.6. |||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Calvert Superbasin. Abbreviated to Carolina Sandstone in both Time-Space Plots.|1863 +/- 6 Ma (maximum depositional age).|Seigal Volcanics.|||Sandstone, siltstone|
26462|Carolina Sandstone Member|69383|4|Described|p48-50|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Up to 20m thick beds. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1863+/-6 Ma|Of Seigal Volcanics||Conformably overlies Westmoreland Conglomerate|Flaggy to massive, fine-grained sandstone, with cross bedding, ripple marks and mud cracks indicating a shallow-marine environment.|
26462|Carolina Sandstone Member|69430|5|Briefly described|p15:3, 10|||Southern McArthur Basin.||Seigal Volcanics.|||A prominent sandstone bed.|12-JUL-16
26462|Carolina Sandstone Member|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Seigal Volcanics||||
26462|Carolina Sandstone Member|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Seigal Volcanics.|||Lithic sandstone and quartz sandstone, fine- to medium-grained, flaggy or massive; minor siltstone beds in the north and conglomerate in the southwest.|
26462|Carolina Sandstone Member|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1863+/-6 Ma (MDA: U-Pb zircon LA-ICPMS).||||Massive cross-bedded sandstone.|
26462|Carolina Sandstone Member|72718|6|Mentioned|p7|||Southern McArthur Basin.||Seigal Volcanics, Tawallah Group||Equivalent to Seigal Volcanics and Sly Creek Sandstone.||
81096|Carrawal Serpentinite|69594|6|Mentioned|p552|||Forms an eastern onlap margin to the Jim Crow Basin.||||||
26297|Carron Rhyolite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Rhyolitic ignimbrite. Overlain by Idalia Rhyolite.||||||15-APR-15
26297|Carron Rhyolite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group.||||||
26297|Carron Rhyolite|23291|4|Described|p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Croydon Volcanic Group. Thickness: 500m. Geological Province: Georgetown Region.||||||15-APR-15
26297|Carron Rhyolite|23430|6|Mentioned|p458 Fig. 14.1|||||||||
26297|Carron Rhyolite|23510|5|Briefly described|Map Legend||Mesoproterozoic|of Croydon Volcanic Group.||||||
26297|Carron Rhyolite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V804. S-Type.||||||
26297|Carron Rhyolite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26297|Carron Rhyolite|40659|2|Defined|p251|Mesoproterozoic|Mesoproterozoic|||||||
26297|Carron Rhyolite|40954|6|Mentioned|p132|||||||||
26297|Carron Rhyolite|41975|5|Briefly described|Table 1 P434|||||||||
26297|Carron Rhyolite|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
26297|Carron Rhyolite|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
26297|Carron Rhyolite|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
26297|Carron Rhyolite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Rhyolitic ignimbrite.||||||15-APR-15
26297|Carron Rhyolite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Nancy Lee Sandstone Member.||Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Nancy Lee Sandstone Member.|Conformably overlies Parrot Camp Rhyolite. Is overlain conformably by Idalia Rhyolite.|Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Conformably overlies B-Creek Rhyolite. Is overlain conformably by Idalia Rhyolite.|Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Conformably overlies B-Creek Rhyolite. Is overlain conformably by Idalia Rhyolite.|Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Conformably overlies B-Creek Rhyolite. Is overlain conformably by Idalia Rhyolite.|Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Conformably overlies B-Creek Rhyolite. Is overlain conformably by Idalia Rhyolite.|Bluish-grey to very dark grey crystal-poor rhyolite ignimbrite with 1 cm crystals, fine eutaxitic texture; flow-banded/laminated phenocryst-poor rhyolite; minor rhyolitic tuff; graphite pellets common.|
26297|Carron Rhyolite|69591|5|Briefly described|p74 Tb.2.5, p75|||Croydon Province, Georgetown Inlier. 500m thick.||Croydon Volcanic Group.|||Crystal-poor rhyolitic ignimbrite; minor sparsely porphyritic rhyolite and medium to coarse, feldspathic sandstone.|
29310|Carrs Granite|23291|5|Briefly described|p102 Tb. 3.13|Early Permian|Late Carboniferous|Of the Ootann Suite. Faulted against Ootann Suite. Age: 283-297 Ma; ~299 Ma. Geological Province: Georgetown Region.||||||08-JUL-15
29310|Carrs Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29310|Carrs Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29310|Carrs Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 320. I-Type.||||||
29310|Carrs Granite|23616|6|Mentioned|p26|||Adjacent to McDevitt Metamorphics||||||
29310|Carrs Granite|24485|5|Briefly described|p13, p61 Tb.10|Late Carboniferous|Late Carboniferous|Intrudes the Dargalong Metamorphics. Parent: Ootann Supersuite||||||
29310|Carrs Granite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Geological Province: Kennedy Province.||||||
29310|Carrs Granite|43060|5|Briefly described|Table 6|||of Ootann Supersuite||||||
29310|Carrs Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
29310|Carrs Granite|43087|2|Defined|p19|Early Permian||Rb-Sr biotite age of 299 Ma. Variation of Carrs Adamellite.||||||
29310|Carrs Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|Late? Carboniferous in age.||||||
29310|Carrs Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type.Grey to pale pink (altered), fine- to medium-grained, slightly porphyritic, hornblende-biotite granite; with scattered enclaves up to ~1m; accessory opaque oxide, zircon, allanite, titanite.||||||07-FEB-11
29310|Carrs Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The three variants are mapped separately.||Unit in Ootann Supersuite.|||Pale pink, fine-grained, porphyritic, biotite monzogranites; leucocratic with large mafic inclusions to ~3 m across; with inclusions to ~1 m across of more mafic granitoid, locally abundant; medium- to fine-grained with muscovite or hornblende.|
36476|Carruchan Monzogranite|23617|4|Described|p21-22|||Also see Table 2 p18 + Table 3 p52. K-Ar 298+/-9 Ma. Kennedy Province.||||||
36476|Carruchan Monzogranite|69593|5|Briefly described|p491-492, p495|Carboniferous|Early Carboniferous|Kangaroo Hills Subprovince, Kennedy Igneous Association. Part of the Bedarra granite belt; exposed on the coast near Ingham.|335 +/- 6 Ma (SHRIMP U-Pb zircon).||||I-type. Dominantly biotite granite; includes hornblende-biotite granite and microgranite; possibly some mafic units.|
30105|Carse Creek Complex|22847|3|Fully described|p 9, 38|||||||||
30105|Carse Creek Complex|23422|5|Briefly described|p173, p209 Table 6.6|Middle Ordovician|Middle Ordovician|Of Columbia Creek Supersuite. Some granites from this complex are included in the Lavery Creek Supersuite.||||||03-DEC-13
30105|Carse Creek Complex|23504|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
30105|Carse Creek Complex|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 204.  A-Type I-Type.||||||
30105|Carse Creek Complex|43093|4|Described|Appendex 1|Ordovician|Late Cambrian|Reserved as Carse Creek Granodiorite.||||||
30105|Carse Creek Complex|43259|4|Described|Appendix 1,p30.|Devonian|Cambrian|Rb-Sr age is 264+/-2 Ma. Cambrian-Devonian possibly also Permian?.||||||03-DEC-13
30105|Carse Creek Complex|43936|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
30105|Carse Creek Complex|68731|6|Mentioned|p149||||||Includes the Jones Dam Suite.||Comprises a mixture of metamorphics and granitoids in the southeastern part of the Ravenswood Batholith.|
30105|Carse Creek Complex|70740|4|Described|p38|Devonian|Cambrian|A type area and reference locality are mentioned from Rienks et al., 1995 and are described. Some of the granites and granodiorites in this complex have an A-type affinity. Metamorphism is discussed briefly. |||||Intermingled medium-grained, subequigranular, biotite-hornblende granodiorite and uniform, grey, subequigranular, fine-grained biotite-muscovite granodiorite that intermingle with rhyolitic hornfels.|
30115|Carse-O-Gowrie Granodiorite|22847|3|Fully described|p 53|Late Silurian||||||||
30115|Carse-O-Gowrie Granodiorite|23422|5|Briefly described|p191, p213 Table 6.8|||See Carse Creek Complex.||||||
30115|Carse-O-Gowrie Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
30115|Carse-O-Gowrie Granodiorite|43093|4|Described|Appendix 1|||Rb-Sr biotite age of 411+/- 2 Ma. Reserved as Carse Creek Granodiorite.||||||
30115|Carse-O-Gowrie Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
30115|Carse-O-Gowrie Granodiorite|62075|6|Mentioned|p15 Fig.7|Late Silurian|Late Silurian|Ravenswood batholith. Appears as Carse-O-Gowrie granodiorite||||||
23476|Casey Spring Creek Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
23476|Casey Spring Creek Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23476|Casey Spring Creek Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 125. I-Type.||||||
23476|Casey Spring Creek Granodiorite|42245|2|Defined|p38|Early Devonian|Late Silurian|||||||
23476|Casey Spring Creek Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23476|Casey Spring Creek Granodiorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Probably related to Medowvale & Five Mile Mill. Late Silurian to Early Devonian?||||||
23476|Casey Spring Creek Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23476|Casey Spring Creek Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Casey Spring Creek gdrt.||Unit in Millchester Supersuite.||||
36617|Cashmere microgranite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36617|Cashmere microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 418.  I-Type.||||||
39614|Cassidy Creek Metamorphics|50201|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
39614|Cassidy Creek Metamorphics|60360|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Mica schist, quartzite, leucogranite.||||||25-JUN-15
39614|Cassidy Creek Metamorphics|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||||
39614|Cassidy Creek Metamorphics|67430|6|Mentioned|p25|||||||||
39614|Cassidy Creek Metamorphics|68330|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Etheridge Province.|||||Mica schist, quartzite; locally abundant leucogranite.|
39614|Cassidy Creek Metamorphics|68331|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Etheridge Province.|||||Mica schist, quartzite; locally abundant leucogranite.|
39614|Cassidy Creek Metamorphics|68346|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Mica schist and quartzite; locally abundant leucogranite.|
39614|Cassidy Creek Metamorphics|68477|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Of the Etheridge Group.|||Mica schist, quartzite; locally abundant leucogranite.|
39614|Cassidy Creek Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. This unit, as well as the Robertson River Subgroup, Juntala and McDevitt Metamorphics, are all mapped under the symbol, -Per.||Unit in Etheridge Group.||||
39614|Cassidy Creek Metamorphics|69591|4|Described|p61-63, p65|Paleoproterozoic|Paleoproterozoic|NE of Einasleigh, Georgetown Inlier. Warnick (1989) described these rocks as part of the Einasleigh Metamorphics. Withnall et al. (2002) showed they were separated by faults and metamorphic grade.||Etheridge Group.||Faulted against Einasleigh Metamorphics. Is intruded by Cobbold Metadolerite.|A belt of mica schist and quartzite; lower metamorphic grade and preserving sedimentary structures.|
39614|Cassidy Creek Metamorphics|70207|6|Mentioned|p14|Paleoproterozoic|Paleoproterozoic|Georgetown region.||||||
73615|Cassilis Granite|65452|6|Mentioned|p6 Fig.2|||Appears as Casilis Granite on p6.||||||
73615|Cassilis Granite|67203|6|Mentioned|p6|Permian|Late Carboniferous|||||||
73615|Cassilis Granite|68679|6|Mentioned|p404|||||||||
73615|Cassilis Granite|73450|6|Mentioned|p21-22|||||||Intruded by Molangul Granite.||
24830|Castletower Granite|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
24830|Castletower Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgct].  Leucocratic hornblende-biotite granite.||||||
24830|Castletower Granite|30451|2|Defined|p85|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
24830|Castletower Granite|30655|6|Mentioned|p39|||||||||
24830|Castletower Granite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
24830|Castletower Granite|35008|6|Mentioned|p178|||||||||
24830|Castletower Granite|35266|6|Mentioned|p204|||||||||
24830|Castletower Granite|36488|6|Mentioned|p4|||See also Plate 1.||||||
24830|Castletower Granite|38447|6|Mentioned|Map legend|Triassic|Permian|Permian to Triassic||||||
24830|Castletower Granite|39445|5|Briefly described|Table 12|||||||||
24830|Castletower Granite|50190|5|Briefly described|p10|Triassic|Permian|||||||
24830|Castletower Granite|67203|5|Briefly described|p4, p11-12|Late Triassic|Permian|Bimodal intrusives. Also appears on p12 as Castle Tower Granite. Two clearly defined episodes of magmatism.|268.1 +/- 1.7 Ma (Cross, unpublished).||||High-level (miarolitic and granophyric) granitoids and fine-grained gabbro and diorite; mixed areas, through extensive net-vein associations, to diverse hybrid rocks.|
24830|Castletower Granite|67874|5|Briefly described|p1-3, p21, p23-24, p27-30, p50|Late Triassic|Late Triassic|Redefined here, based on geochronology. Previously mapped as a single extensive unit between Lake Awonga (in the N), and headwaters of Boyne and Kolan Rivers (in the S). Now divided into Castletower Granite (northernmost pluton), Many Peaks Granite (central areas), and Bulburin Granite (southern regions). SHRIMP U-Pb zircon magmatic crystallisation age.|221.8 +/- 1.3 Ma (SHRIMP U-Pb zircon).||||Pale pink, fine- to medium-grained, uneven-grained, leucocratic alkali feldspar granite; scattered granophyric intergrowths and miarolitic cavities up to ~2.5cm across.|
24830|Castletower Granite|68008|3|Fully described|p2, p199, p326-330, p416-418, p491, p616|||Dear et al. (1971). Named after Mount Castletower. No type area. Forms a number of separate plutons in a 45 x 10 km belt SSE from Lake Awonga. Crops out as high, extremely rugged timbered country. Geochemistry detailed: similar to Miriam Vale Granodiorite; both share similarities with Winterbourne and Coulston Volcanics, and to Robert and Molangul Granites. May be mid-Permian. Hosts the Mount Jacob Goldfield deposits. Geophysics modelling.||||Intrudes Calliope beds, Wandilla Formation and ?Miriam Vale Granodiorite. Is intruded by Norton Tonalite. Is ?overlain nonconformably by Bobby Volcanics.|Almost sole rock type is a pink to buff, medium-grained, equigranular, leucocratic syenogranite.|
24830|Castletower Granite|68679|5|Briefly described|p337, p422, p428, p431-432|Late Triassic|Late Triassic|Northern New England Orogen; Gladstone area. Forms steep, rugged terrain in the Castletower Range. Previously mapped as an extensive unit; largely replaced by Many Peaks Granite, leaving a smaller pluton.|221.8 +/- 1.3 Ma (SHRIMP: Cross et al., 2012).||||Leucocratic hornblende-biotite granite.|
24830|Castletower Granite|68901|6|Mentioned|p145|||||||||26-SEP-18
24830|Castletower Granite|72481|6|Mentioned|p429|||Topographically prominent occurrence between Rockhampton and Bundaberg.||||||
24830|Castletower Granite|73197|6|Mentioned|p477|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase. Shown as Castle Tower Granite on p476.|269 or 268 Ma U-Pb|||||
24830|Castletower Granite|73450|4|Described|p4, p7, p9-10, p37|Norian|Norian|Previously included several plutons along the Many Peaks Range from Lake Awoonga to the Boyne River headwaters; now restricted to the relatively large, discrete, northern-most pluton located south of Lake Awoonga. Forms relatively high, extremely rugged country. Yielded a U-Pb SHRIMP zircon crystallisation age of 222 +/- 1 Ma (Cross et al., 2012).|222 +/- 1 Ma U-Pb SHRIMP|||Intrudes Calliope beds, Wandilla Formation, Jackass Gabbro, and Many Peaks Granite.|Includes pale pink to buff, fine- to medium-grained, uneven-grained, leucocratic alkali feldspar granite.|
27040|Caterpillar Microgranite|23291|5|Briefly described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Newcastle Range A-types. Geological Province: Georgetown Region.||||||27-MAY-15
27040|Caterpillar Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 25.||||||
27040|Caterpillar Microgranite|23619|4|Described|p39 Table 2||Carboniferous|Intrudes Einasleigh Metamorphics, Puppy Camp Granodiorite and Eveleigh Volcanic Subgroup. Also see p10. Georgetown Province.||||||
27040|Caterpillar Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27040|Caterpillar Microgranite|40542|6|Mentioned|p97|||||||||
27040|Caterpillar Microgranite|43113|4|Described|Table 2 p25||Carboniferous|||||||
27040|Caterpillar Microgranite|43253|5|Briefly described|map legend||Carboniferous|||||||
27040|Caterpillar Microgranite|43259|4|Described|Appendix 1, p17.||Carboniferous|||||||24-SEP-14
27040|Caterpillar Microgranite|43740|5|Briefly described|p16|||||||||
27040|Caterpillar Microgranite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||||||
27040|Caterpillar Microgranite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
27040|Caterpillar Microgranite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27040|Caterpillar Microgranite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Microgranite.||||||
27040|Caterpillar Microgranite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous||||||Grey to brown, abundantly porphyritic microgranite with sparse chlorite.|
27040|Caterpillar Microgranite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to brown, abundantly porphyritic microgranite with sparse chlorite.|
27040|Caterpillar Microgranite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to brown, abundantly porphyritic microgranite with sparse chlorite.|27-MAY-15
27040|Caterpillar Microgranite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Grey to brown, abundantly porphyritic microgranite with sparse chlorite.|
27040|Caterpillar Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned.|||||A-type. Porphyritic microgranite, rhyolite grading to microgranite, biotite granite.|
36179|Catherine Creek Granodiorite|23506|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Almaden Supersuite.||||||
36179|Catherine Creek Granodiorite|60425|4|Described|p282-3 Appdx.|Early Permian|Late Carboniferous|Uanssigned. I-type. Grey, medium-grained, even-grained biotite-hornblende granodiorite to monzogranite.||||||07-FEB-11
80768|Cathu Granodiorite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Granodiorite.|
36176|Cattle Camp Granite|23506|5|Briefly described|Map Legend||Early Permian|of O'Briens Creek Supersuite.||||||
36176|Cattle Camp Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Cherry Tree Suite (O'Briens Creek Supersuite). I-type. Detailed lith.included (monzogranite/syenogranite). Delineated as discrete unit (Wild River granite) by Clarke (1990, 1995); included in Saint Patrick Hill Granite by Donchak and Bultitude (1998).||||||07-FEB-11
25839|Cattle Creek Formation|13516|5|Briefly described|p145 fig 3, p147 fig 5, p148-151|Early Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP22 - APP32|||Mostyndale Mudstone Member, Riverstone Sandstone Member, Moorooloo Mudstone Member, Staircase Sandstone Member, Sirius Mudstone Member|Overlies or lateral marine equivalent of Reids Dome beds; paralic.||
25839|Cattle Creek Formation|22969|5|Briefly described|p 21||Permian|Bowen Basin||||||
25839|Cattle Creek Formation|22973|5|Briefly described|p9 Fig.2 (b)|Early Permian|Early Permian|||||||
25839|Cattle Creek Formation|22975|5|Briefly described|p34 Fig.6|Early Permian|Early Permian|||||||
25839|Cattle Creek Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
25839|Cattle Creek Formation|22980|5|Briefly described|p249 Fig.2|Early Permian|Early Permian|||||||
25839|Cattle Creek Formation|22993|5|Briefly described|p330 Table 1|Permian|Early Permian|||||||
25839|Cattle Creek Formation|23006|5|Briefly described|p447|||||||||
25839|Cattle Creek Formation|23060|5|Briefly described|16|||Geol Province: Bowen Basin.||||||30-NOV-09
25839|Cattle Creek Formation|24077|5|Briefly described|p410 Tb. 2|Early Permian|Early Permian|Of the Tiverton Subgroup.  Max. thickness: 910m.  Geological Province: Bowen Basin.||||||
25839|Cattle Creek Formation|29391|6|Mentioned|Table 3|||See P18.||||||
25839|Cattle Creek Formation|29393|6|Mentioned|Table 2|||Permian.||||||
25839|Cattle Creek Formation|29410|6|Mentioned|p274|||Geological map. Permian.||||||
25839|Cattle Creek Formation|29412|6|Mentioned|p209|||Also Fig.2.||||||
25839|Cattle Creek Formation|29436|6|Mentioned|p317|||||||||
25839|Cattle Creek Formation|29437|6|Mentioned|p154|||||||||
25839|Cattle Creek Formation|29721|6|Mentioned|p65|||||||||
25839|Cattle Creek Formation|30153|6|Mentioned|p151|||Fauna correlates with Cascades Group, Tasmania.||||||
25839|Cattle Creek Formation|30340|6|Mentioned|p2532|||Lithology||||||
25839|Cattle Creek Formation|30341|4|Described|p136|||Lower Permian age||||||
25839|Cattle Creek Formation|30449|6|Mentioned|p2|||||||||
25839|Cattle Creek Formation|30450|6|Mentioned|Table 1|||Permian age||||||
25839|Cattle Creek Formation|30545|6|Mentioned|p22|||[Wrong State? Originally recorded as in WA. CEBFeb95]||||||
25839|Cattle Creek Formation|30546|6|Mentioned|p107|||Lower Permian age. Correlation||||||
25839|Cattle Creek Formation|30826|6|Mentioned|Fig.1|||||||||
25839|Cattle Creek Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
25839|Cattle Creek Formation|30916|6|Mentioned|p98|||||||||
25839|Cattle Creek Formation|31079|6|Mentioned|Fig. 6|||||||||
25839|Cattle Creek Formation|31120|4|Described|p149|||||||||
25839|Cattle Creek Formation|31303|6|Mentioned|p292|||||||||
25839|Cattle Creek Formation|31305|4|Described|p568|||Mention Table 1||||||
25839|Cattle Creek Formation|31396|6|Mentioned|p1185|||||||||
25839|Cattle Creek Formation|31621|6|Mentioned|p151|||||||||
25839|Cattle Creek Formation|32096|6|Mentioned|p574|||||||||
25839|Cattle Creek Formation|32139|6|Mentioned|p579|||||||||
25839|Cattle Creek Formation|32577|4|Described|p23|||See also P24,27,32,33,42. L.Perm.||||||
25839|Cattle Creek Formation|32837|6|Mentioned|p170|||Refers Paten (1969)||||||
25839|Cattle Creek Formation|32840|6|Mentioned|p29|||Stratigraphy & biostratigraphy||||||
25839|Cattle Creek Formation|32943|6|Mentioned|Fig.2|||See also PP94,106||||||
25839|Cattle Creek Formation|32945|6|Mentioned|p81|||See also Fig.3||||||
25839|Cattle Creek Formation|33366|6|Mentioned|Fig.3|||Perm.||||||
25839|Cattle Creek Formation|33711|6|Mentioned|p383|||See also Table 3.||||||
25839|Cattle Creek Formation|33745|6|Mentioned|p204|||See also Figs 2 & 3||||||
25839|Cattle Creek Formation|34099|6|Mentioned|p10|||||||||
25839|Cattle Creek Formation|34132|6|Mentioned|p5|||Lower Permian||||||
25839|Cattle Creek Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian - Artinskian||||||
25839|Cattle Creek Formation|34170|6|Mentioned|p48|||Lower Permian||||||
25839|Cattle Creek Formation|34415|6|Mentioned|p82|||||||||
25839|Cattle Creek Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
25839|Cattle Creek Formation|35079|6|Mentioned|p424|||||||||
25839|Cattle Creek Formation|35148|6|Mentioned|p410|||||||||
25839|Cattle Creek Formation|35150|6|Mentioned|p420|||||||||
25839|Cattle Creek Formation|35160|6|Mentioned|p1|||||||||
25839|Cattle Creek Formation|35284|6|Mentioned|Fig.1|||||||||
25839|Cattle Creek Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
25839|Cattle Creek Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
25839|Cattle Creek Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
25839|Cattle Creek Formation|35845|6|Mentioned|p65|||||||||
25839|Cattle Creek Formation|35862|6|Mentioned|p282|||||||||
25839|Cattle Creek Formation|35873|6|Mentioned|p116|||||||||
25839|Cattle Creek Formation|35901|6|Mentioned|p28|||||||||
25839|Cattle Creek Formation|36103|4|Described|Table 1|||||||||
25839|Cattle Creek Formation|36104|6|Mentioned|p122|||||||||
25839|Cattle Creek Formation|36233|4|Described|p155|||See also Table 1.||||||
25839|Cattle Creek Formation|36241|4|Described|p115|||||||||
25839|Cattle Creek Formation|36243|6|Mentioned|Table 3A|||||||||
25839|Cattle Creek Formation|36549|5|Briefly described|p519|||||||||
25839|Cattle Creek Formation|36739|6|Mentioned|Fig.2|||||||||
25839|Cattle Creek Formation|36899|6|Mentioned|p1091|||||||||
25839|Cattle Creek Formation|37070|6|Mentioned|p69|||||||||
25839|Cattle Creek Formation|37139|6|Mentioned|p78|||||||||
25839|Cattle Creek Formation|37450|4|Described|p374|||||||||
25839|Cattle Creek Formation|37610|6|Mentioned|Fig.4|||||||||
25839|Cattle Creek Formation|37612|6|Mentioned|p283|||See also Fig.3||||||
25839|Cattle Creek Formation|37705|6|Mentioned|Fig.2|||||||||
25839|Cattle Creek Formation|37724|6|Mentioned|Table 1|||||||||
25839|Cattle Creek Formation|37726|3|Fully described|p138|||||||||
25839|Cattle Creek Formation|37918|6|Mentioned|p474|||||||||
25839|Cattle Creek Formation|38092|6|Mentioned|p284|||||||||
25839|Cattle Creek Formation|38198|6|Mentioned|p414|||||||||
25839|Cattle Creek Formation|38204|6|Mentioned|p77|||||||||
25839|Cattle Creek Formation|38312|4|Described|p458|||||||||
25839|Cattle Creek Formation|38444|6|Mentioned|p302|||||||||
25839|Cattle Creek Formation|38518|6|Mentioned|Fig.3|||||||||
25839|Cattle Creek Formation|38917|6|Mentioned|p155|||||||||
25839|Cattle Creek Formation|38955|4|Described|p312|||||||||
25839|Cattle Creek Formation|39212|5|Briefly described|p11|||P24-gas reservoir||||||
25839|Cattle Creek Formation|39219|6|Mentioned|p46|||Microflora||||||
25839|Cattle Creek Formation|39252|6|Mentioned|Fig.13|||||||||
25839|Cattle Creek Formation|39253|6|Mentioned|p34|||||||||
25839|Cattle Creek Formation|39256|5|Briefly described|p53|||||||||
25839|Cattle Creek Formation|39261|6|Mentioned|Fig.6|||||||||
25839|Cattle Creek Formation|39262|6|Mentioned|p126|||||||||
25839|Cattle Creek Formation|39263|6|Mentioned|p139|||||||||
25839|Cattle Creek Formation|39264|6|Mentioned|Fig. 4|||||||||
25839|Cattle Creek Formation|39273|4|Described|p305|||||||||
25839|Cattle Creek Formation|39275|6|Mentioned|p332|||||||||
25839|Cattle Creek Formation|39412|6|Mentioned|p6|||||||||
25839|Cattle Creek Formation|39423|6|Mentioned|p47|||||||||
25839|Cattle Creek Formation|39445|5|Briefly described|Table 8|||||||||
25839|Cattle Creek Formation|39494|6|Mentioned|Fig.5|||||||||
25839|Cattle Creek Formation|39611|6|Mentioned|Fig.2|||||||||
25839|Cattle Creek Formation|39813|6|Mentioned|Map legend|Permian|Carboniferous|Permo Carboniferous||||||
25839|Cattle Creek Formation|39815|6|Mentioned|p443|||||||||
25839|Cattle Creek Formation|39943|6|Mentioned|Table 5A|||||||||
25839|Cattle Creek Formation|39994|6|Mentioned|p200|||See also P201||||||
25839|Cattle Creek Formation|40030|6|Mentioned|p137|||||||||
25839|Cattle Creek Formation|40093|6|Mentioned|p26|||||||||
25839|Cattle Creek Formation|40250|6|Mentioned|Table 6|||||||||
25839|Cattle Creek Formation|40539|6|Mentioned|Fig.2|||||||||
25839|Cattle Creek Formation|40544|6|Mentioned|Fig.6|||||||||
25839|Cattle Creek Formation|40675|6|Mentioned|Table 5A|||||||||
25839|Cattle Creek Formation|41173|6|Mentioned|p92|||||||||
25839|Cattle Creek Formation|41191|6|Mentioned|Fig.3|||||||||
25839|Cattle Creek Formation|41246|6|Mentioned|Map legend|Permian||||||||
25839|Cattle Creek Formation|41247|6|Mentioned|p128|||See also Fig.7||||||
25839|Cattle Creek Formation|41275|4|Described|p30|||||||||
25839|Cattle Creek Formation|41330|6|Mentioned|Table 1|||||||||
25839|Cattle Creek Formation|41514|5|Briefly described|p68|||||||||
25839|Cattle Creek Formation|41605|6|Mentioned|p29|||||||||
25839|Cattle Creek Formation|41639|6|Mentioned|p7|||||||||
25839|Cattle Creek Formation|41666|6|Mentioned|p10|||||||||
25839|Cattle Creek Formation|41689|6|Mentioned|Table 1|||||||||
25839|Cattle Creek Formation|41737|6|Mentioned|p351|||||||||
25839|Cattle Creek Formation|41920|6|Mentioned|Inside back cover|||||||||
25839|Cattle Creek Formation|41949|4|Described|p115|||||||||
25839|Cattle Creek Formation|42000|6|Mentioned|p55|||||||||
25839|Cattle Creek Formation|42249|6|Mentioned|p21|||||||||
25839|Cattle Creek Formation|42250|6|Mentioned|Fig.4 P31|||||||||
25839|Cattle Creek Formation|42252|6|Mentioned|Fig.1 P47|||||||||
25839|Cattle Creek Formation|42253|5|Briefly described|Fig.2 P217|||||||||
25839|Cattle Creek Formation|42254|6|Mentioned|p221|||||||||
25839|Cattle Creek Formation|42437|5|Briefly described|p820|||||||||
25839|Cattle Creek Formation|42578|6|Mentioned|Table 1 P124-125|||||||||
25839|Cattle Creek Formation|42621|5|Briefly described|p274|||||||||
25839|Cattle Creek Formation|42641|6|Mentioned|Fig.3 P110|||||||||
25839|Cattle Creek Formation|42808|5|Briefly described|p156|||see also Fig.1 P157||||||
25839|Cattle Creek Formation|42856|6|Mentioned|p640|||||||||
25839|Cattle Creek Formation|42865|5|Briefly described|p18|||||||||
25839|Cattle Creek Formation|42911|6|Mentioned|p8|||||||||
25839|Cattle Creek Formation|42974|6|Mentioned|p202|||||||||
25839|Cattle Creek Formation|43000|5|Briefly described|Fig.5,p112|||||||||
25839|Cattle Creek Formation|43017|5|Briefly described|Fig.3,p375|||||||||
25839|Cattle Creek Formation|43050|5|Briefly described|p4|||see also Fig.1,p5.||||||
25839|Cattle Creek Formation|43185|5|Briefly described|6-8||Early Permian|||||||
25839|Cattle Creek Formation|43204|5|Briefly described|Map Legend|Early Permian|Early Permian|||||underlies Aldebaran Sandstone||23-DEC-11
25839|Cattle Creek Formation|43213|5|Briefly described|p10, p69, p152|||120m thick.|||||Burrowed and fossiliferous, marine, quartzose to sublabile sandstone and sandy siltstone.|
25839|Cattle Creek Formation|43475|14|Not recorded|p553||Permian|||||||
25839|Cattle Creek Formation|43580|6|Mentioned|Fig.1,p360|||||||||
25839|Cattle Creek Formation|43714|6|Mentioned|Fig.3,p5||Early Permian|||||||
25839|Cattle Creek Formation|43737|6|Mentioned|p5||Kungurian|||||||
25839|Cattle Creek Formation|43812|6|Mentioned|Fig.3,p145|||||||||
25839|Cattle Creek Formation|43977|14|Not recorded|p576|||See also Lexicon.||||||
25839|Cattle Creek Formation|43987|14|Not recorded|p266,270|||||||||
25839|Cattle Creek Formation|43990|14|Not recorded|Map Legend|||Part of Tiverton Sub-Group.||||||
25839|Cattle Creek Formation|43995|14|Not recorded|Tb.p9,15-9,53,fig.6,||Permian|Equivalent to Sirius Shale. Figs.8,14.||||||
25839|Cattle Creek Formation|44000|14|Not recorded|p32|||Correlated with Tiverton Formation, Equivalent to Sirius Formation, Staircase Formation, Stanleigh Formation.||||||
25839|Cattle Creek Formation|44022|14|Not recorded|Map Legend||Early Permian|||||||
25839|Cattle Creek Formation|44023|4|Described|Tb.2,p6||Early Permian|||||||
25839|Cattle Creek Formation|44074|14|Not recorded|p183|||||||||
25839|Cattle Creek Formation|44079|14|Not recorded|p50,51|||||||||
25839|Cattle Creek Formation|44081|14|Not recorded|Pl.9|||||||||
25839|Cattle Creek Formation|44085|2|Defined|Opp.p4,9,10,15,17|||||||||
25839|Cattle Creek Formation|44091|14|Not recorded|p45,Tb.3,p47|||Part of Middle Bowen Group in Springsure area.||||||
25839|Cattle Creek Formation|44115|14|Not recorded|p19,21|||||||||
25839|Cattle Creek Formation|44169|2|Defined|p6,7,Tb.1,map|||||||||
25839|Cattle Creek Formation|44170|4|Described|p5,6,8,10,29,30,32,||Early Permian|Tb.1||||||
25839|Cattle Creek Formation|44172|2|Defined|p1320,1323,1325,1327||Artinskian|p1329,1330-4,1336,1340,1342-3. Denison Trough.||||||
25839|Cattle Creek Formation|44173|14|Not recorded|p109-113||Artinskian|||||||
25839|Cattle Creek Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
25839|Cattle Creek Formation|44348|14|Not recorded|p55||Artinskian|||||||
25839|Cattle Creek Formation|44349|14|Not recorded|p64|||||||||
25839|Cattle Creek Formation|44381|14|Not recorded|p5|||||||||
25839|Cattle Creek Formation|44419|14|Not recorded|p272,273||Permian|||||||
25839|Cattle Creek Formation|44421|14|Not recorded|p8,map||Permian|||||||
25839|Cattle Creek Formation|44422|14|Not recorded|p151,152||Early Permian|||||||
25839|Cattle Creek Formation|44424|14|Not recorded|p293-301|||In Tiverton Subgroup.||||||
25839|Cattle Creek Formation|44426|14|Not recorded|p11|||||||||
25839|Cattle Creek Formation|44488|14|Not recorded|p48|||||||||
25839|Cattle Creek Formation|44489|14|Not recorded|p70,71|||||||||
25839|Cattle Creek Formation|44604|14|Not recorded|p116|||||||||
25839|Cattle Creek Formation|44618|14|Not recorded|p517 (Fig.5)||Permian|||||||
25839|Cattle Creek Formation|44651|14|Not recorded|p117,124|||||||||
25839|Cattle Creek Formation|44855|14|Not recorded|p27||Permian|||||||
25839|Cattle Creek Formation|44857|14|Not recorded|p97,98||Permian|||||||
25839|Cattle Creek Formation|44858|14|Not recorded|p94||Artinskian|||||||
25839|Cattle Creek Formation|44859|14|Not recorded|p70||Permian|Peruvispira.||||||
25839|Cattle Creek Formation|45016|14|Not recorded|p.18|||Glaciation.||||||
25839|Cattle Creek Formation|45031|14|Not recorded|p9,10,20,23,28,72,74|||p88,100,102,Fig.3,Pl.1,2,||||||
25839|Cattle Creek Formation|45071|3|Fully described|Table 6|||||||||
25839|Cattle Creek Formation|45110|3|Fully described|Table 14|||||||||
25839|Cattle Creek Formation|46849|6|Mentioned|p192|||||||||
25839|Cattle Creek Formation|46989|5|Briefly described|Table 1|||||||||
25839|Cattle Creek Formation|48600|14|Not recorded|p13|||Springsure area.||||||
25839|Cattle Creek Formation|48626|4|Described|p1,3,22,24,46-50,54,||Permian|p55,58,103,Pl.1,Fig.2||||||
25839|Cattle Creek Formation|48630|14|Not recorded|p1,4,5,7,8,13,18,19,|||p22,Pls.1,2.||||||
25839|Cattle Creek Formation|48831|14|Not recorded|p.17,18,32,87,88|||||||||
25839|Cattle Creek Formation|48841|14|Not recorded|p20|||||||||
25839|Cattle Creek Formation|48845|14|Not recorded|p30,37,38|||||||||
25839|Cattle Creek Formation|48898|6|Mentioned|Fig.4|||L.Permian||||||
25839|Cattle Creek Formation|48900|2|Defined|p27|Early Permian|Early Permian|||||||
25839|Cattle Creek Formation|48919|5|Briefly described|Table 2|||L.Permian||||||
25839|Cattle Creek Formation|48971|6|Mentioned|p9|||See also P12, P15, P18, P23.||||||
25839|Cattle Creek Formation|48995|6|Mentioned|Fig.3|||||||||
25839|Cattle Creek Formation|49644|5|Briefly described|Table|||||||||
25839|Cattle Creek Formation|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
25839|Cattle Creek Formation|60286|5|Briefly described|p274|Early Permian|Early Permian|Overlies Reids Dome Beds. Overlain by Lower Aldebaran Sandstone.||||||
25839|Cattle Creek Formation|60330|5|Briefly described|p261 Fig.2|Kungurian|Artinskian|||||||11-MAY-05
25839|Cattle Creek Formation|60369|5|Briefly described|Map Legend|Early Permian|Early Permian|Overlies Reids Dome Beds. Overlain by Aldebaran Sandstone. Fossiliferous sandy mudstone (subsurface only).||||||03-SEP-04
25839|Cattle Creek Formation|60386|6|Mentioned|p296|Artinskian|Artinskian|Bowen/Sydney Basin. Deltaic - nearshore - shelf. ||||||
25839|Cattle Creek Formation|61313|6|Mentioned|p104 Table G1|||||||||
25839|Cattle Creek Formation|61377|6|Mentioned|p156 Tb. SU2|Early Permian|Early Permian|A reservoir unit in Queensland.||||||07-FEB-11
25839|Cattle Creek Formation|61612|6|Mentioned|p270, p271, p270 Fig. 1|Early Permian|Early Permian|Includes Sirius Mudstone Member. Geological Province: Denison Trough. QLD.||||||17-MAR-09
25839|Cattle Creek Formation|62357|5|Briefly described|p524 Fig. 7, p531|Middle Permian|Early Permian|Geological Province: Bowen Basin.||||||
25839|Cattle Creek Formation|63172|6|Mentioned|p305|||In Queensland.||||||07-FEB-11
25839|Cattle Creek Formation|63713|5|Briefly described|p1507 Fig.2, p1508|Kungurian|Artinskian|Denison Trough, Bowen Basin.||||Is overlain by Aldebaran Sandstone.||
25839|Cattle Creek Formation|63832|6|Mentioned|p131 fig 2, p136|Cisuralian|Cisuralian|Draper (1983). Of Bowen Basin. Sixth (P2) glaciation; predominantly glaciomarine facies.||||||13-DEC-17
25839|Cattle Creek Formation|64631|5|Briefly described|p44 Fig.2, p48 Fig.4, p49.|Artinskian|Sakmarian|Bowen Basin. Predominantly glaciomarine facies. Biostratigraphic age control for base and top. Base shown as time transgressive, Sakmarian to Artinskian, oldest in W, on p44.||||Overlies Reids Dome Beds. Is overlain by Lower Aldebaran Sandstone.||
25839|Cattle Creek Formation|64665|6|Mentioned|p53 Fig.2.|Early Permian|Early Permian|Bowen Basin.||||Overlies Reids Dome beds. Is overlain by Aldebaran Sandstone.||
25839|Cattle Creek Formation|64856|6|Mentioned|p49|||Denison Trough. Upper part correlated with Buffel Formation| | ||||31-JAN-13
25839|Cattle Creek Formation|64857|5|Briefly described|p116, p113 Fig.3||Early Permian|Bowen Basin. Overlies Reids Dome beds. Age implied from underlying relationship with Aldebaran Sandstone. Age: late Early Permian||||||
25839|Cattle Creek Formation|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Unit in the Denison Trough, Bowen Basin. Underlies Aldebaran Sandstone.||||||22-MAR-12
25839|Cattle Creek Formation|65113|5|Briefly described|p338, p345, Fig 4 p 340|Early Permian|Early Permian|Denison Trough. Equivalent to the  top of Early Permian volcanic pile in the Taroom Trough. Has wide spread layer cake geometry. Overlies the Reids Dome beds, Underlies the lower Aldebaran Sandstone.||||||
25839|Cattle Creek Formation|65114|5|Briefly described|p385 Fig.3|Early Permian||||||||
25839|Cattle Creek Formation|65115|5|Briefly described|p409, 411, Fig 2 p403|Early Permian|Artinskian|Underlies the lower Aldebaran Sandstone, overlies the Reids Dome beds in the Denison Trough, Bowen Basin. Part of Supersequence B.||||||
25839|Cattle Creek Formation|65116|5|Briefly described|p442, Fig 2 p436|Early Permian|Early Permian|Underlies the lower Aldebaran Sandstone and overlies the Reids Dome beds in the Denison Trough in the Bowen Basin.||||||
25839|Cattle Creek Formation|65118|5|Briefly described|p480, 487, Fig 2 p479|Permian|Permian|Underlies the lower Aldebaran Sandstone in the Denison Trough, Bowen Basin.||||||
25839|Cattle Creek Formation|66188|6|Mentioned|443|Early Permian|Early Permian|||||||
25839|Cattle Creek Formation|66615|6|Mentioned|p2 Fig.1|||Denison Trough, Bowen Basin.||||||
25839|Cattle Creek Formation|67402|4|Described|p21, p23 fig CTM3|Kungurian|Artinskian|Bowen Basin. Approximately 380m thick. Deposited in a marine environment. See also p64 fig BWW2, p65, p66 fig BWW4, p69, P71-p73, p85 tbl BWN2.|||Includes the Staircase Sandstone and Riverstone Sandstone.|Overlain by the Aldebaran Sandstone, Lower. Overlies the Reids Dome beds.|Sandstone, siltstone and mudstone. Sandstone beds are commonly thick.|
25839|Cattle Creek Formation|67669|5|Briefly described|p11|Early Permian|Early Permian|Of Bowen Basin.||||Overlain by Aldebaran Siltstone. Underlain by Reid Dome beds or Timbury Hills Formation.||
25839|Cattle Creek Formation|68576|5|Briefly described|Q_4: p3, p7, p19|Cisuralian|Cisuralian|Price (1997). Bowen Basin. Displays cross-stratification, flame structures, soft sediment deformation, slump folds and dewatering structures.|||Includes Sirius Mudstone, Staircase Sandstone, Mostydale Mudstone, Riverstone Sandstone, Moorooloo Mudstone Members.|Is overlain by Aldebaran Sandstone.|Marine, fossiliferous, conglomeratic and silty sandstone, with thin interbeds of limestone and calcareous sandstone.|22-OCT-19
25839|Cattle Creek Formation|68679|5|Briefly described|p375, p378-379, p381, p384, p469|Permian|Permian|Mollan et al. (1969). Bowen Basin. 800m thick. Marine shelf, delta sediments. Widely deposited during a thermal relaxation event. Produces gas and minor condensate.|c.280 Ma.|||Overlies and interfingers with Reids Dome beds. Is overlain gradationally by Aldebaran Sandstone.|Quartzose sandstone, mudstone, siltstone, coal; marine fossils (the Formation contains three Mudstone Members and two Sandstone Members).|
25839|Cattle Creek Formation|68731|6|Mentioned|p201 Fig 3.110, p206|Cisuralian|Cisuralian|Bowen Basin.|||Includes the Sirius Mudstone Member.|||
25839|Cattle Creek Formation|70815|6|Mentioned|p3|||Bowen Basin.||||||
25839|Cattle Creek Formation|70856|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group.||Overlain by Aldebaran Sandstone, overlies Reids Dome beds.|Quartzose to sublabile sandstone and mudstone.|
25839|Cattle Creek Formation|71265|5|Briefly described|p589|Cisuralian|Cisuralian|Bowen Basin.|||Sirius Mudstone Member.|Overlies Reids Dome beds. Is overlain by Aldebaran Sandstone.||
25839|Cattle Creek Formation|71701|5|Briefly described|p155, p170|Kungurian|Artinskian|Denison Trough, Bowen Basin.|||Includes the Sirius Mudstone Member.|Unconformably overlies the Reids Dome beds. Overlain by the Aldebaran Sandstone, lower.||
25839|Cattle Creek Formation|72088|5|Briefly described|p8, p91|Kungurian|Artinskian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Faulted against the Reids Dome beds. Unconformably overlain by the Sirius Mudstone Member.||
25839|Cattle Creek Formation|72297|5|Briefly described|p694 Fig.10.8, p745|Permian|Permian|Bowen Basin. Oil and gas source rock.||||||
25839|Cattle Creek Formation|73113|5|Briefly described|p. 1, 19-20, 22, 24, 26, 28, 30-32...|Early Permian|Early Permian|Bowen Basin, Denison Trough. Coal seam gas target reservoir. Groundwater model divided the unit into a non-productive zone and upper and lower layers. Interbedded aquitard. Not considered laterally extensive across the basin. More locations: p. 37-38, 41, 49, 51-52, 59, 88, 97-101, 103-105, 107, 117, 119, 123-124, 132, 134, 146-148, 150, 152, 154, 172, 174-175, 178-179, 191.||||Unconformably overlain by Precipice Sandstone.||
25839|Cattle Creek Formation|73304|6|Mentioned|p78|||Bowen Basin, southern.||||||
25839|Cattle Creek Formation|73472|6|Mentioned|p115|Kungurian|Artinskian||||Sirius Mudstone Member|Underlain by and equivalent to Reids Dome beds. Overlain by Aldebaran Sandstone.||
25839|Cattle Creek Formation|73625|6|Mentioned|p3|Permian|Permian|Bowen Basin.||||||
33141|Cecilwood Quartz Diorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgce].  Hornblende quartz diorite.||||||
33141|Cecilwood Quartz Diorite|50208|5|Briefly described|Map Legend|Triassic|Permian|||||||14-MAY-04
33141|Cecilwood Quartz Diorite|68008|3|Fully described|p82, p395-397, p621-622, p624|Triassic|Permian|New name. Previously mapped as unnamed Permian granodiorite by Kirkegaard et al. (1970). A 10 x 8km intrusion, 23km S of Bajool. Named after Cecilwood homestead. No type area; deeply weathered and outcrops are rare. Forms very flat topography. Geophysics described and modelled; part of the Bajool Gravity Low. Geochemistry briefly described. No age data. Hosts thorium-rich skarns.||||Intrudes Mount Alma Formation, Raspberry Creek Formation and (presumably) Ginger Creek beds.|Greenish-grey, medium-grained, equigranular quartz diorite.|
33141|Cecilwood Quartz Diorite|68679|5|Briefly described|p424-425|||Yarrol Province. A ~10 x 8 km intrusion.||||Intrudes Ginger Creek Member (Raspberry Creek Formation) and Mount Alma Formation.|Hornblende quartz diorite. Th-rich skarns at contact at southern side; magnetic images highlight hornfelsed rim and suggest two lobes.|
73616|Cedarvale Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Coarse-grained, porphyritic biotite granite with rapakivi texture.|
73616|Cedarvale Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Coarse-grained, porphyritic biotite granite with rapakivi textures.|
73616|Cedarvale Granite|73450|6|Mentioned|p16|||||||||
26335|Centauri Granodiorite|22847|3|Fully described|p 49|||||||||
26335|Centauri Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
26335|Centauri Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 474.  Assumed to be I-Type.||||||
26335|Centauri Granodiorite|42633|5|Briefly described|Table 1 P8|||See also misspelling Centuri..||||||
26335|Centauri Granodiorite|42750|2|Defined|p43|Early Devonian|Late Silurian|||||||
26335|Centauri Granodiorite|43093|4|Described|Appendix 1|||May be Middle Silurian to Early Devonian||||||
26335|Centauri Granodiorite|43259|4|Described|Appendix 1,p50.|Early Devonian|Late Silurian|||||||
26335|Centauri Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26335|Centauri Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Centauri gdrt.||Unit in Millchester Supersuite.||||
26335|Centauri Granodiorite|62521|5|Briefly described|p23, p55|Early Devonian|Late Silurian|Of Millchester Creek Supersuite. Geological Province: Ravenswood Batholith. Deeply weathered unit. See also p18.||||||14-JAN-08
69008|Ceratodus Granite|61087|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Eidsvold Complex. Pale grey to white, fine to medium-grained equigranular leucocratic biotite granite.||||||
69008|Ceratodus Granite|64399|5|Briefly described|Map legend|Late Permian|Late Permian|Part of the Edsvold Complex.. Fine- to medium-grained equigranular leucocratic biotite granite.||||||
69008|Ceratodus Granite|65388|4|Described|p293-294. 289, 290, 300|Early Permian|Early Permian|New unit within Eidsvold Complex. Relationship with Harkness Granodiorite and Mount Rose Gabbro is uncertain. K-Ar biotite age of  241 Ma may be reset. Generally pink to light grey, fine to medium-grained granite or granodiorite; equigranular to porphyritic.||||||
69008|Ceratodus Granite|68679|5|Briefly described|p408|Permian|Permian|Auburn Subprovince, New England Orogen. Relationship to other Eidsvold Complex rocks uncertain.||Eidsvold Complex.|||Pink to light grey, fine- to medium-grained, equigranular granite with some granodiorite.|
35110|Cerberus Rhyolite Member|23042|4|Described|p32,3,4, Fig 2||Early Permian|Now mapped as part of the Mount Benmore Volcanics.||||||
35110|Cerberus Rhyolite Member|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pvbc].  Grey, moderately crystal-rich (feldspar and minor quartz), lithic-rich rhyolitic to dacitic ignimbrite.||||||
35110|Cerberus Rhyolite Member|50213|5|Briefly described|Map legend|Permian|Permian|Of the Mount Benmore Volcanics.  Mainly rhyolitic to dacitic ignimbrite and subordinate volcaniclastic sediments.||||||17-MAY-04
35110|Cerberus Rhyolite Member|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Mount Benmore Volcanics (Lizzie Creek Volcanic Group). Grey, moderatly crystal rich to crystal rich, lithic rich rhyolitic to dacitic ignimbrite.||||||
35110|Cerberus Rhyolite Member|65388|3|Fully described|p126-127; p84, 86, 118, 121, 122, 124|Early Permian|Early Permian|Of Mount Benmore Volcanics,  Lizzie Creek Volcanic Group. Type area:  top of the plateau at Mount Gardiner, where it is overlain by the upper part of the Mount Benmore Volcanics. The base overlies mafic volcanics of the Mount Benmore Volcanics. Bluish grey, crystal-rich volcaniclastic rocks, inferred to be mainly ignimbrite. Also spelt Cerberus Dacite Member on p 126.||||||
35110|Cerberus Rhyolite Member|68679|5|Briefly described|p358|||Mount Gardiner Plateau, south Connors Subprovince.||Mount Benmore Volcanics.|||A prominent unit, one of the rare thin felsic ignimbrite sheets in the mafic to intermediate Mount Benmore Volcanics.|
27641|Chadshunt Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|porphyritic garnet-biotite granite with metasedimentry xenoliths and graphitic inclusions near margins.||||||02-JUL-04
27641|Chadshunt Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||04-JUN-15
27641|Chadshunt Granite|23510|5|Briefly described|Map Legend||Mesoproterozoic|of Esmeralda Supersuite.||||||
27641|Chadshunt Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 803. S-Type.||||||
27641|Chadshunt Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27641|Chadshunt Granite|40659|6|Mentioned|p250|||||||||
27641|Chadshunt Granite|40954|6|Mentioned|p132|||||||||
27641|Chadshunt Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
27641|Chadshunt Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Porphyritic (muscovite-) biotite-garnet granite with abundant metasedimentary (generally carbonaceous) xenoliths and graphitic inclusions near margins.|
27641|Chadshunt Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Porphyritic (muscovite-) biotite-garnet granite with abundant metasedimentary (generally carbonaceous) xenoliths and graphitic inclusions near margins.|
27641|Chadshunt Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Coarse biotite granite with trace secondary muscovite; contains garnet. Abundant enclaves and disseminated graphite, especially near the roof of the pluton.|
33435|Chahpingah Meta-Igneous Complex|23799|3|Fully described|p21, p15 Tb. 1|Permian|Late Carboniferous|Of the Yarraman Subprovince (Wandilla Province).  Age: 301Ma (Cranfield and others, 1998) - concordant with Mountefontein Metamorphics.  Intruded by Boondooma Igneous Complex.||||||
33435|Chahpingah Meta-Igneous Complex|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
33435|Chahpingah Meta-Igneous Complex|50384|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: Yarraman Subprovince.||||||
33435|Chahpingah Meta-Igneous Complex|60371|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: Yarraman Subprovince. Banded granitic to granodioritic biotite gneiss||||||
33435|Chahpingah Meta-Igneous Complex|63821|6|Mentioned|p15|||Mapped in the Gympie area.||||||07-FEB-11
33435|Chahpingah Meta-Igneous Complex|68679|4|Described|p321-324, p403-405, p470-471|Late Carboniferous|Late Carboniferous|Formally described by Cranfield et al. (2001) after studies by Hubbard (1985) and Holcombe et al. (1997). Yarraman Subprovince, northern New England Orogen. Forms two large adjoining lobate outcrop areas (each ~100 km2) 40km W of Kingaroy. Lithology described in some detail. Lower plate component of an extensional complex, produced by subduction rollback to the east. Forms a deformed sheet-like body in western Yarraman Subprovince. Several similarities to Wratten Igneous Suite. Age history described.|~303 Ma (U-Pb zircon: Cranfield et al. (1998).|||Is intruded by Boondooma Igneous Complex. Probably intruded and enclosed Mountefontein Metamorphics. Is overlain unconformably by Main Range Volcanics. Correlated with Hillgrove Suite.|Mainly cream to grey, fine- to medium-grained, strongly foliated, banded granitic to granodioritic biotite gneiss; quartz veins and ptygmatically folded pegmatite veins (?migmatitic), pegmatite and granite dykes, sills and small intrusions. S-type.|
33435|Chahpingah Meta-Igneous Complex|73197|6|Mentioned|p471|Guadalupian|Late Carboniferous|New England Orogen. Intrudes the Wandilla province. Contemporaneous with rifting in late Carboniferous-Middle Permian. See also Chahpingah Complex p470.||||||
38892|Chalmers Formation|24420|5|Briefly described|p7|Early Permian|Early Permian|Of Berserker Group.||||||
38892|Chalmers Formation|24615|5|Briefly described|CD|Permian|Permian|[Pkc].  Siltstone, lithic sandstone, rhyolitic to andesitic volcaniclastic breccia, rhyolitic and dacitic tuff, minor andesitic tuff.||||||
38892|Chalmers Formation|50207|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||
38892|Chalmers Formation|50208|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||
38892|Chalmers Formation|50212|5|Briefly described|Map Legend|Permian|Permian|Of Berserker Group.  Contains the Sleipner Member.||||||17-MAY-04
38892|Chalmers Formation|60557|5|Briefly described|p25, p36-37|Early Permian|Early Permian|Well-bedded sequence of siltstone and sandstone, intruded by sills of basalt.||||||09-JUN-05
38892|Chalmers Formation|61778|3|Fully described|p234 Fig. 1, p235-256, p240 Fig. 11||Early Permian|Of Berserker Group. Unconformably underlain by Rockhampton Gp. Age: 277+/-4Ma (U-Pb). Consists of interbedded sediments and rhyolitic to andesitic volcaniclastics. Geological Province: Berserker Subprovince. See p235-236 for detailed lithology.||||||07-FEB-11
38892|Chalmers Formation|64429|2|Defined|p15, p19-21|Early Permian|Early Permian|Of Berserker Gp.Contains Sleipner Mbr.Unconform.on Rockhampton Gp.Lateral facies equiv.of Lakes Ck Fm.Faulted against Yarwun beds.Thickness: ~600m. Detailed lithol.included - of siltstones/sandstones+pyroclastic rocks and granule-pebble volcanic breccia||||||
38892|Chalmers Formation|68008|2|Defined|p113,p158,p160, p163-167, p170, p172-173|Permian|Permian|See also p527. New name, after Mount Chalmers. The type area, 300m S of Mount Archer, is from GR252267 7416546 to GR251747 7415695. Fossils listed. Thickness ~600m. Hosts base metal and gold deposits. Geochemistry described.|277.1 +/- 3.5 Ma (U-Pb zircon).|Berserker Group.|Sleipner Member.|Equivalent to, locally overlies, Lakes Creek Formation. Unconformably overlies Rockhampton Group. Correlative of Buffel Formation.|Siltstone, sandstone, pyroclastic rocks, granule to pebble volcanic breccia, local thick-bedded calcareous sandstone; local schist and tectonite adjacent to the Yarrol Fault.|
38892|Chalmers Formation|68679|5|Briefly described|p318, p350|Permian|Permian|Berserker Subprovince, Yarrol Province. Similar to Lakes Creek Formation. Includes a succession of shallowly dipping felsic tuff and breccia previously named the Balnagowan Volcanic Member (Doonside Formation), at Balnagowan homestead W of the Yarrol Fault.||Berserker Group.|Sleipner Member.||Siltstone and sandstone, with medium- to very thick-bedded volcaniclastic rocks; fossiliferous grey-green, medium- to thick-bedded sandstone and granule to pebble breccia; a thick fossiliferous calcareous sandstone bed.|
38892|Chalmers Formation|71592|5|Briefly described|Appendix A.|||New England Orogen.|||||Volcanic breccia.|
39079|Champion Hills Diorite|23799|3|Fully described|p92, p12 Tb. 1|Triassic|Triassic|Of the South-east Queensland Volcanic and Plutonic Intrusives.  See also "Champion Hills Diorite".  Intrudes Buaraba Mudstone (Cressbrook Creek Gp.); intruded by South Buaraba Microdiorite dykes.  Gabbro, diorite, pyroxenite, basic diorite, quartz diorite||||||
39079|Champion Hills Diorite|68679|5|Briefly described|p414|||Hegarty (1981). West of the Esk Basin, northern New England Orogen.|||||Forms numerous bodies of fine- to coarse-grained, equigranular, porphyritic and subophitic gabbro, dolerite, pyroxenite, diorite and quartz diorite.|
31010|Channer Creek beds|24488|5|Briefly described|Map Legend|Late Devonian|Late Devonian|||||||
31010|Channer Creek beds|24615|5|Briefly described|CD|Late Devonian|Late Devonian|[Da].  Lithic sandstone, siltstone, conglomerate.||||||
31010|Channer Creek beds|43461|14|Not recorded|table p618||Frasnian|||||||
31010|Channer Creek beds|64399|5|Briefly described|Map legend|Late Devonian|Late Devonian|Lithic sandstone, siltstone, conglomerate.||||||
31010|Channer Creek beds|68008|4|Described|p48-50, p109, p603|Frasnian|Frasnian|Named by Dear et al. (1971) for marine beds with Frasnian faunas mapped by Maxwell (1960). Crops out as low hills, 8.5 km x 2.5 km along W side of the Yarrol Fault. Disrupted by numerous faults: stratigraphic relationships are unknown. Fossil species, corals listed: age implications briefly discussed. Location and strong magnetic signature are similar to Calliope beds.||||Is faulted against Rockhampton Group to the W, and against Doonside and Wandilla Formations to the E. Correlated with Lochenbar and Mount Hoopbound Formations.|Dark green, fine- to coarse-grained lithic sandstone and granule to pebble conglomerate; rare light green argillite. Local andesitic lava and siliceous fine-grained sandstone recorded.|
31010|Channer Creek beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Balaclava, Lochenbar and Mount Hoopbound Formations, the Tanderra Volcanics and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
31010|Channer Creek beds|68679|5|Briefly described|p312-313, p340|Early Carboniferous|Late Devonian|Northern New England Orogen. Crops out in a fault-bounded strip 20km long and up to 2.5km wide, due E of Mulgildie and straddling Poperima Creek and Burnett River. Frasnian and Givetian corals indicate erosion of underlying Formations.|||||Mainly lithic sandstone (andesite and plagioclase grains), granule to pebble conglomerate (andesite clasts) and rare argillite. Andesitic lavas and fine-grained siliceous sandstone reported.|
80929|Charles Creek Granite|69592|5|Briefly described|p283|||Copperfield Batholith. Unassigned.|||||Muscovite-biotite leucogranite to leucogranodiorite; biotite leucogranite. Probably I-type (no analytical data).|
36529|Charlesford complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 184.||||||
80223|Charlie Creek Microgranite|70740|4|Described|p106 fig 62b, p120-p122, p125|Permian|Carboniferous|Interpreted as a high-level late-stage intrusive phase of the Kennedy Igneous Association. Distribution is briefly discussed on p122. Age assumed from map symbol used, and broad discussion of the Kennedy Igneous Province.||||Intrudes the Collins Creek Rhyolite and the Hidden Valley Rhyolite.|Pink to orange-brown, coarsely porphyritic biotite microgranite to microsyenogranite.|05-OCT-17
77809|Charlies Knob Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Medium-grained biotite granite.|
23482|Charlotte Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|Of Cooktown Supersuite. Age: 275 +/- 5Ma.||||||01-JUN-09
23482|Charlotte Granite|42369|3|Fully described|p46|Late Permian||Previously mapped as Findlayson Granite. Age K-Ar about 260Ma.||||||
23482|Charlotte Granite|42474|5|Briefly described|p27|||||||||
23482|Charlotte Granite|43070|2|Defined|p14||Early Permian|Of Cooktown Supersuite. Age: late Early Permian||||||01-JUN-09
23482|Charlotte Granite|50587|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Geological Province: Kennedy Province. Fine to medium grained, tourmaline-muscovite-biotite-granite.||||||28-JUN-04
23482|Charlotte Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Early Permian|Of Cooktown Suite (Cooktown Supersuite). S-type. Age: 275+/-5Ma (SHRIMP); 278-262Ma (Rb-Sr, est.).Fine- to med.gr.(garnet-)cordierite (altered)- tourmaline-muscovite-biotite granite; scattered enclaves and miarolitic cavities - more lithol. detail incl.||||||07-FEB-11
23482|Charlotte Granite|69593|5|Briefly described|p479, p481 Fig.6.5(b), p482, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Dating by Bultitude et al. (1997). Sm-Nd isotope data tabulated.|275 +/- 5 Ma (SHRIMP U-Pb zircon).|Cooktown Suite.|||S-type granitoids.|
23482|Charlotte Granite|72983|6|Mentioned|p3, p31|Roadian|Kungurian|Similar age to the Collingwood Granite date from Murgulov (2006).|275 +/- 5 Ma SHRIMP U-Pb|Cooktown Supersuite|||S-type granites.|
78914|Charon Point Rhyolite Member|65388|3|Fully described|p70-73; p70 Fig.28; p73 Fig.29; p58, 69|Early Carboniferous|Late Devonian |Of Campwyn Subprovince, Yarrol Province. Of Tanderra Volcanics. Misspelt on the SAINT LAWRENCE map as Charons Point Rhyolite Member. Spelling is Charon Point. SHRIMP age of 352 +/- 5 Ma obtained for ignimbrite in the Charon Point Rhyolite Member. Type  at Charon Point (MGA 788990 7522010.||||||
78914|Charon Point Rhyolite Member|68679|5|Briefly described|p348|Tournaisian|Tournaisian|Campwyn Subprovince, Northern Yarrol Province. See also reference to Charons Point Rhyolite Member (p308).|352 +/- 5 Ma (U-Pb zircon: Withnall et al., 2009).|Tanderra Volcanics.|||Ignimbrites.|
78914|Charon Point Rhyolite Member|71592|5|Briefly described|Appendix A.||||352+/-4.9 Ma (SHRIMP U-Pb zircon).||||Ignimbrite.|
35856|Chase Point Meta-andesite|23330|5|Briefly described|1078-9, 1083|Triassic|Early Permian|Formerly Chase Point Metabasalt. Revised here. Minimum age (metamorphic age): 230 +/-10 Ma K/Ar. Maximum age (age of crystallisation of amphobole in diorite in Chase Point meta-andesite): 277+/-7 Ma.|||||Greenish-grey fine-grained equigranular andesitic pillow lavas, metamorphosed to greenschist facies.|10-JUL-13
35856|Chase Point Meta-andesite|63600|5|Briefly described|p902|||Also presented as the compound name, Chase Point Metabasalt or Meta-andesite; C.P. Metabasalt probably the formal name.||||||07-FEB-11
41263|Cheltenham Creek Granite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Porphyritic hornblende-biotite monzogranite, foliated biotite granodiorite.||||||30-JUN-04
41263|Cheltenham Creek Granite|65388|3|Fully described|p302-307, p301, 321, 329, 338, 339-340|Middle Triassic|Early Triassic|Replaces most of Cheltenham Creek Adamellite. Distribution modified from Whitaker & others (1974). Of Wingfield Suite. Intrudes Narayen beds. Appears to be intruded in the north by the Pollard Granodiorite. In contact with (probably older) Delubra Gabbro. K-Ar ages 244+/-8 Ma (hornblende) and 245+/-7Ma (biotite). Mainly pink to grey coarse-grained porphyritic hornblende-biotite monzogranite, with common to abundant alkali feldspar phenocrysts to 4cm. High K2O.||||||04-SEP-14
41263|Cheltenham Creek Granite|68679|5|Briefly described|p416, p418, p420|||Southern part of the Rawbelle Batholith. Elliptical pluton with an outcrop area ~30 km2. Also appears as Chelternham Creek Granodiorite on p418. Geochemistry plot.|245 +/- 7 Ma (K-Ar: Whitaker et al., 1974).|||Intrudes Delubra Gabbro. Is intruded by Pollard Granodiorite.|Porphyritic hornblende-biotite monzogranite; minor foliated biotite granodiorite; relatively homogeneous with abundant alkali feldspar megacrysts.|
36173|Cherry Tree Granite|23506|5|Briefly described|Map Legend||Early Permian|of O'Briens Creek Supersuite.||||||
36173|Cherry Tree Granite|60425|4|Described|p45 Tb. 3, p284-5 Appdx.|Early Permian|Early Permian|Of Cherry Tree Suite (O'Briens Ck Sup'suite).Cuts Walsh Bluff Volcs. Detailed lithology for this biotite granite included; I-type. Delineated as discrete unit by Clarke (1990, 1995); included in Saint Patrick Hill Granite by Donchak and Bultitude (1998).||||||07-FEB-11
69335|Cherry Tree Suite|60425|5|Briefly described|p73, p284-5 Appdx. |Early Permian|Late Carboniferous|Of O'Briens Creek Supersuite. Contains Cherry Tree, Specimen Hill, Kauri, Cattle Camp and Herberton Hill Granites. I-types.||||||07-FEB-11
68149|Cherwell Mudstone Member|60281|5|Briefly described|p37, p40|Cretaceous|Cretaceous|Of the Maryborough Formation.  Carbonaceous shale.  Overlies the basal Gregory Sandstone Member.  Geological Province: Maryborough Basin. See Fig. 30 Appendix 1.||||||
68149|Cherwell Mudstone Member|61611|5|Briefly described|p266|Early Cretaceous|Early Cretaceous|Of Maryborough Formation. Overlies Gregory Sandstone. Geological Province: Maryborough Basin.||||||13-MAR-09
28035|Chevy Creek Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group and Burton Lagoon Granite||||||
28035|Chevy Creek Granite|43596|4|Described|p31,  p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Oswald and Annie Creek Schists, Burton Lagoon Granite. Pale grey to cream, abundantly porphyritic muscovite-biotite granite; euhedral phenocrysts of muscovite and K-feldspar. Porly exposed except in Chevy Ck.||||||07-APR-15
28035|Chevy Creek Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
69588|Childers Volcanics|61155|5|Briefly described|p20|Early Oligocene|Early Oligocene|Age: 32.5-30.5Ma. In the Bundaberg-Maryborough region. Not related to Childers Formation in the Gippsland Basin. ||||||
30014|China Camp Microgranite|43070|3|Fully described|p93|||||||||
30014|China Camp Microgranite|43625|4|Described|p56,126,Appendix 7|||||||||
30014|China Camp Microgranite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Roaring Meg Suite (Cooktown Supersuite). S-type. Pale brown, fine-grained, slightly porphyritic tourmaline-biotite-muscovite granite; miarolitic cavivites and tourmaline-rich aggregates common; associated with tin mineralisation at China Camp.||||||07-FEB-11
30014|China Camp Microgranite|69593|5|Briefly described|p479, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Appears as China Camp Granite on p511.|270 Ma.|Roaring Meg Suite.|||S-type granitoids.|
27078|Chinaman Creek Limestone|23032|5|Briefly described|p27 fig6|Devonian|Devonian|||||||
27078|Chinaman Creek Limestone|23424|5|Briefly described|Table 8.1 p335|Givetian|Emsian|Prev. referred to as 'Pandanus Carbonate Platform'  Mawson & Tabeut (1989). Sloan et al (1995) proposed reamalgamation into 1 unit, Chinaman Ck Lmst? Seems to have been ignored. Of  Wandovale Subgp. Tank Ck Sndste underlying unit. Graveyard Ck Subprovinc||||||03-JUL-14
27078|Chinaman Creek Limestone|24577|5|Briefly described|p754 Fig. 2|Devonian|Devonian|Of the Broken River Group. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
27078|Chinaman Creek Limestone|24611|6|Mentioned|p225|||Geological Province: Broken River Province.||||||
27078|Chinaman Creek Limestone|24613|6|Mentioned|p131|||Geological province: Broken River Province. Referred to as lower Chinaman Creek Limestone.||||||07-FEB-11
27078|Chinaman Creek Limestone|41260|3|Fully described|p67|||Described P118||||||
27078|Chinaman Creek Limestone|41679|1|Redefined|p256|Givetian|Emsian|||||||
27078|Chinaman Creek Limestone|41719|6|Mentioned|Fig.2|||||||||
27078|Chinaman Creek Limestone|41739|6|Mentioned|Fig.2|||||||||
27078|Chinaman Creek Limestone|42015|6|Mentioned|p318|||||||||
27078|Chinaman Creek Limestone|42031|5|Briefly described|Fig.5 P762|||||||||
27078|Chinaman Creek Limestone|42032|5|Briefly described|p500|||||||||
27078|Chinaman Creek Limestone|42054|6|Mentioned|p273|||||||||
27078|Chinaman Creek Limestone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
27078|Chinaman Creek Limestone|42933|1|Redefined|Table 2|Middle Devonian|Early Devonian|See also p86||||||
27078|Chinaman Creek Limestone|50088|5|Briefly described|p473|||One specimen of Belodella staufferi - in Broken River area. Specimen age is Late Emsian.||||||
27078|Chinaman Creek Limestone|50093|5|Briefly described|p329 Fig.2, p330 Fig.3|Givetian; late varcus subzone (conodont)|Emsian; inversus zone (conodont)|Of Broken River Group.||||||07-FEB-11
27078|Chinaman Creek Limestone|68336|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and lesser calcilutite; subordinate calcareous siltstone, mudstone and quartzose to lithic arenite and pebble conglomerate.|
27078|Chinaman Creek Limestone|68341|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and lesser calcilutite; subordinate calcareous siltstone, mudstone and quartzose to lithic arenite and pebble conglomerate.|
27078|Chinaman Creek Limestone|68731|6|Mentioned|p187|Middle Devonian|Lower Devonian|||||Correlative of the Conjuboy Formation.||
27078|Chinaman Creek Limestone|69592|4|Described|p264, p273-274|Givetian|Emsian|Pandanus Creek area; Graveyard Creek Subprovince, Broken Creek Province. Now (Talent et al., 2002) includes the Dip Creek, Jessey Springs and Lockup Well Limestones (Wyatt and Jell, 1980; Lang et al., 1993) as part of a laterally continuous lithofacies. Up to 790m thick. Lithologies and fossils more fully described. NW of Pandanus Creek, the Bulgeri Formation wedges out into this unit.||Wandovale Subgroup.||Is locally overlain unconformably by Bulgeri Formation.|Mainly clastic limestone intervals (individually up to 250m thick) of calcirudite and calcarenite with packstone, grainstone and wackestone fabrics; sporadic thin interbeds of calcareous mudstone, siltstone and sandstone; micritic lime mud interbeds.|
36191|Chinamans Creek Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
25844|Chinchilla Sand|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
25844|Chinchilla Sand|29428|6|Mentioned|p31|||||||||
25844|Chinchilla Sand|29429|6|Mentioned|p37,38|||||||||
25844|Chinchilla Sand|29433|6|Mentioned|p384|||||||||
25844|Chinchilla Sand|29673|6|Mentioned|p309|||Late Pliocene||||||
25844|Chinchilla Sand|29674|6|Mentioned|p373|||||||||
25844|Chinchilla Sand|29675|6|Mentioned|p46|||||||||
25844|Chinchilla Sand|29677|6|Mentioned|p370|||||||||
25844|Chinchilla Sand|30582|6|Mentioned|p9|||Kangaroo remains||||||
25844|Chinchilla Sand|30638|6|Mentioned|p232||Pliocene|||||||
25844|Chinchilla Sand|30692|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
25844|Chinchilla Sand|30698|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
25844|Chinchilla Sand|31333|6|Mentioned|p20|||||||||
25844|Chinchilla Sand|32007|6|Mentioned|p155|||||||||
25844|Chinchilla Sand|32636|6|Mentioned|p34|||See also P35. Pliocene?||||||
25844|Chinchilla Sand|32797|4|Described|Table 5|||Pliocene||||||
25844|Chinchilla Sand|34906|6|Mentioned|p1|||||||||
25844|Chinchilla Sand|34976|6|Mentioned|p127|||||||||
25844|Chinchilla Sand|34996|6|Mentioned|p145|||||||||
25844|Chinchilla Sand|38371|6|Mentioned|p657|||||||||
25844|Chinchilla Sand|38373|6|Mentioned|p623|||||||||
25844|Chinchilla Sand|38374|6|Mentioned|p606|||||||||
25844|Chinchilla Sand|39445|5|Briefly described|Table 14|||See also Fig 11.6||||||
25844|Chinchilla Sand|40129|6|Mentioned|p177|||||||||
25844|Chinchilla Sand|40623|5|Briefly described|p73|||||||||
25844|Chinchilla Sand|40910|6|Mentioned|p19|||||||||
25844|Chinchilla Sand|41537|6|Mentioned|p352|||||||||
25844|Chinchilla Sand|43008|5|Briefly described|map legend|||||||||
25844|Chinchilla Sand|43889|14|Not recorded|p116,125|||Fossil macropodids, Darking Downs.||||||
25844|Chinchilla Sand|44252|14|Not recorded|p394|||This name replaces Chinchilla Formation.||||||
25844|Chinchilla Sand|44377|14|Not recorded|p20|||||||||
25844|Chinchilla Sand|44731|14|Not recorded|unknown (p139-143)|||Not listed on white card.||||||
25844|Chinchilla Sand|44829|6|Mentioned|p33|||||||||
25844|Chinchilla Sand|45110|2|Defined|p151|Pliocene|Pliocene|Formerly Chinchilla Formation (Woods,1956). See also Table 21.||||||
25844|Chinchilla Sand|45128|6|Mentioned|p56|||||||||
25844|Chinchilla Sand|48917|6|Mentioned|p41|||Pliocene vertebrates||||||
25844|Chinchilla Sand|61007|5|Briefly described|p293|Pliocene|Pliocene|Characterised by vertebrate fossils. ||||||
25844|Chinchilla Sand|61155|5|Briefly described|p5, p19|Late Pliocene|Early Pliocene|Fluvial clastic deposits. Thickness: 90m. Geological Province: eastern Surat Basin.||||||
25844|Chinchilla Sand|65003|6|Mentioned|p16||Pliocene|||||||
25844|Chinchilla Sand|69599|5|Briefly described|p580, p602|Pliocene|Pliocene|Woods (1960). Crops out immediately SE of Chinchilla and extends along the Condamine River to Warra. Up to 30m thick in surface exposures; much thicker subsurface. Contains an abundant and well-studied vertebrate fossil fauna.|||||Coarse clastics.|
25844|Chinchilla Sand|73200|5|Briefly described|p532 Fig.1, p533, p542 Fig.14|Pliocene|Pliocene|Deposited along relict drainage features north of the Condamine Valley, preceded Quaternary fluvial-alluvial deposits of a meandering river system.|||||Alluvium.|
26258|Chipley Granite|22847|3|Fully described|p 43|Ordovician|Ordovician|||||||
26258|Chipley Granite|23422|5|Briefly described|p173|||Of Chipley Supersuite.  Probably Ordovician.||||||
26258|Chipley Granite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
26258|Chipley Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 86. Assumed to be I-Type.||||||
26258|Chipley Granite|42750|2|Defined|p36|Middle Ordovician||||||||
26258|Chipley Granite|43093|4|Described|Appendix 1||Ordovician|Middle Ordovician||||||
26258|Chipley Granite|43259|4|Described|Appendix 1,p21.||Ordovician|||||||
26258|Chipley Granite|43933|5|Briefly described|Map Legend||Ordovician|||||||
26258|Chipley Granite|62521|5|Briefly described|p12, p25-26|Middle Ordovician|Late Cambrian|Of the Hogsflesh Creek Supersuite. Geological Province: Ravenswood Batholith. A well defined ovoid pluton that intrudes Lavery Creek Granite. Comprises quartz, albite, orthoclase, biotite, muscovite, garnet, chlorite, epidote and allanite.||||||14-JAN-08
26258|Chipley Granite|68731|5|Briefly described|p149|||Previously included in the Hogsflesh Creek Supersuite by Hutton and Crouch (1993a, 1993b), but Hutton et al. (1994a, 1994b) separated it out on the basis of a lower K2O, low K2O/Na2O and high P2O5.||Of the Chipley Suite.||||
38218|Chipley Suite|23422|5|Briefly described|p209 Table 6.6|||Age: Probably Ordovician.||||||
38218|Chipley Suite|62521|5|Briefly described|p25|Ordovician|Ordovician|Of the Hogsflesh Creek Supersuite. Includes Chipley Granite. ||||||
38218|Chipley Suite|68731|6|Mentioned|p148, p149|Ordovician|Ordovician|A tentative Ordovician age is assigned on the basis of strain textures.|||Includes the Chipley Granite.|||
34666|Chipley Supersuite|22847|6|Mentioned|p 10|||||||||
34666|Chipley Supersuite|23422|4|Described|p173|Ordovician|Ordovician|See also Chipley Suite p209 table 6.6.||||||
34666|Chipley Supersuite|23430|5|Briefly described|p481 Fig 14.6|||Ravenswood Batholith Province.||||||
34666|Chipley Supersuite|23893|5|Briefly described|p13|Middle Ordovician|Late Cambrian|Geological Province: Macrossan Province.||||||
34666|Chipley Supersuite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Brittany, Columbia Creek (part), Hogsflesh and Lavery Creek Supersuites; Schreibers and Sunburst Suites; the Lynwater Complex; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
79732|Choc-a-block Orthogneiss|71792|2|Defined|p3, p6, p8, p11-p13, p39|Mesoproterozoic|Mesoproterozoic|Savannah Province. Named for the Choc-A-Block Creek which trends to the southwest of the known outcrop of the orthogneiss. The type locality is sample site DPCY031 at 143.0223'E, 13.02481'S east of the Portland Roads Road in the Mangkuma Land Trust area. Occurs on the western flank of the Weymouth Granite. Previously mapped as part of the Kintore Granite, on the basis of geochronology this unit has been redefined as part of the Coen Metamorphic Group. Age is a SHRIMP date interpreted as the metamorphic crystallisation age of this unit; maximum depositional ages of the protolith are provided by Cross et al (in prep) as 1632 +/- 27 Ma. This unit has a moderate magnetic response and exhibits pale pink tones in radiometrics; in both cases it is difficult to distinguish from the surrounding units. Petrographic description provided.|1585 +/- 4.4 Ma (Cross et al, in prep)|Coen Metamorphic Group||Unconformably overlain by the Janet Ranges Volcanics. Overlain by the Goolha Goolha Schist. Intruded by the Kintore and Weymouth supersuites.|Medium to coarse-grained, strongly foliated biotite orthogneiss.|
79732|Choc-a-block Orthogneiss|72983|5|Briefly described|p5-7, p104-109, p116|Statherian|Statherian|Iron Range Province. Eastern Cape York region. New ages led to a sampled outcrop mapped as Kintore Granite being reassigned to this unit. Metamorphic age of 1585.1 +/- 4.4 Ma. Age is the best estimate for the timing of an early Mesoproterozoic regional metamorphic event. Possible thermal influenced from the Kintore Granite.|1632 +/- 27 Ma SHRIMP U-Pb|Coen Metamorphic Group|||Foliated granitic gneiss.|
79732|Choc-a-block Orthogneiss|73387|6|Mentioned|p1|Statherian|Statherian|Maximum depositional age of 1632 +/- 27 Ma from Cross et al. (2019).|1632 +/- 27 Ma|Coen Metamorphic Group||||
78567|Chong beds|68731|6|Mentioned|p201 Fig 3.110|Late Triassic|Late Triassic|Bowen Basin.||||||
78567|Chong beds|69594|5|Briefly described|p519, p535, p545, p572|Rhaetian|Rhaetian|Northern Surat Basin. Price (1995, 1997) named the Taroom beds; to avoid confusion with Taroom Coal Measures, Price's unit is here called the Chong beds.||||?Is overlain unconformably by Precipice Sandstone.||
78567|Chong beds|69633|5|Briefly described|p3, p11|Early Jurassic|Early Jurassic|Surat Basin.||||Is overlain unconformably by Precipice Sandstone.||
78567|Chong beds|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Surat Basin.||||||
78567|Chong beds|70374|6|Mentioned|p809 figure 1|Sinemurian|Hettanginian|||||||
40847|Christmas Hill Trondhjemite|50200|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
40847|Christmas Hill Trondhjemite|68410|5|Briefly described|Map Legend|Late Silurian|Late Silurian||||||Grey, foliated, porphyritic biotite trondhjemite or leucotonalite.|
40847|Christmas Hill Trondhjemite|69592|6|Mentioned|p283|Silurian|Silurian|||Dido Supersuite.||||
23487|Chulcee Formation|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Inorunie Group.||||||02-JUL-04
23487|Chulcee Formation|23291|4|Described|p83 Tb. 3.6|Early Paleozoic|Mesoproterozoic|Parent: Inorunie Group. Thickness: 250m? Geological Province: Georgetown Region.||||||04-JUN-15
23487|Chulcee Formation|40218|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
23487|Chulcee Formation|40954|6|Mentioned|p132|||||||||
23487|Chulcee Formation|41975|6|Mentioned|Fig.3 P433|||||||||
23487|Chulcee Formation|43664|6|Mentioned|Fig.3,p15|||||||||
23487|Chulcee Formation|68355|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Dirie Sandstone. Is overlain conformably by Guela Sandstone.|Dark red-brown, variably ferruginous, micaceous lithic-quartz siltstone and fine sandstone, laminated mudstone, shale and minor orthoquartzite.|
23487|Chulcee Formation|68356|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Dirie Sandstone. Is overlain conformably by Guela Sandstone.|Dark red-brown, variably ferruginous, micaceous lithic-quartz siltstone and fine sandstone, laminated mudstone, shale and minor orthoquartzite.|
23487|Chulcee Formation|69591|6|Mentioned|p75|||Croydon Province, Georgetown Inlier.||Inorunie Group.||||
23489|Cigarette Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||01-JUN-09
23489|Cigarette Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 272. I-Type.||||||
23489|Cigarette Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
23489|Cigarette Granite|41235|6|Mentioned|Fig.2a|||||||||
23489|Cigarette Granite|41740|6|Mentioned|p222|||||||||
23489|Cigarette Granite|43259|4|Described|Appendix 1,p35.||Carboniferous|||||||
23489|Cigarette Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Age: ~315-313Ma. Pale pink, fine-grained, porphyritic (topaz-) biotite granite; with associated Sn mineralisation. I-type.||||||07-FEB-11
25845|Claravale Sandstone Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
25845|Claravale Sandstone Member|30695|4|Described|Table 4|||Lower Cretaceous . Unit of Bungil Formation||||||
25845|Claravale Sandstone Member|30702|6|Mentioned|p49|||See also p51. Stratigraphic Table||||||07-OCT-15
25845|Claravale Sandstone Member|44022|14|Not recorded|Map Legend||Early Cretaceous|||||||
25845|Claravale Sandstone Member|44023|4|Described|Tb.3,p12||Early Cretaceous|||||||
25845|Claravale Sandstone Member|45110|4|Described|p111|||See also p110. Of Bungil Formation.||||||07-OCT-15
25845|Claravale Sandstone Member|48919|2|Defined|p70|Early Cretaceous|Early Cretaceous|See also p71. L.Cretaceous||||||07-OCT-15
25845|Claravale Sandstone Member|64856|5|Briefly described|p98|Early Cretaceous|Early Cretaceous|Mollan et al. (1972). Member of the Bungil Formation. Merrivale Syncline, W Surat Basin.| | ||||28-NOV-17
25845|Claravale Sandstone Member|69594|5|Briefly described|p538|||Mollan et al. (1972). Western Surat Basin.||Bungil Formation.||||
82627|Clare Hills Monzogranite|71628|3|Fully described|p19: 58-60, 63-67, 70-71|||New name. Previously Clare Hills Granite (Donchak et al., 2007) and Herries Monzogranite (Brown et al., 2007). Largely equivalent to the Ruby Creek Leucogranite of Robertson (1971) and Olgers et al. (1972). Named after a local homestead. Type locality is MGA 382899 6866415 (Allora 1:100,000 sheet) (Donchak et al., 2007). Crops out as a ~9 x 3 km body ~23 km WSW of Warwick. Forms scattered boulders and tors. Geochemistry described, and assigned to Herries Suite. Minor Au-Pb mineralisation occurs in quartz veins.|252 +/- 2.5 Ma (SHRIMP: Li et al., 2012).|Granite Hills Complex.||Intrudes Texas beds. Abuts Fairleigh Monzogranite.|Pale pinkish-grey to grey, fine- to medium-grained, slightly to moderately porphyritic, hornblende-biotite monzogranite; finer-grained and porphyritic marginal variants. I-type.|
74066|Clare Hills Suite|63748|5|Briefly described|p34|||Of the Herries Supersuite. Includes Clare Hills Granite.||||||07-FEB-11
74066|Clare Hills Suite|68679|5|Briefly described|p456, p460|||Northern New England Batholith. ~19 km2.||Stanthorpe Supersuite.|Clare Hills Granite.|||
74066|Clare Hills Suite|71628|5|Briefly described|p19: 60, 63|||Redefined in this study; different from the original Suite of Donchak et al. (2007) within the Herries Supersuite.||Herries Supersuite.|Clare Hills Granite.|||
29977|Claret Creek Supersuite|23423|4|Described|p314 Table 7.4|Early Permian|Late Carboniferous|I-type. Age: 300 +/- 5 Ma, 290 Ma (Rb-Sr). Also see p240. Kennedy Igneous Province.||||||
29977|Claret Creek Supersuite|23430|5|Briefly described|p497|||||||||
29977|Claret Creek Supersuite|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
29977|Claret Creek Supersuite|23616|5|Briefly described|p74-75|||I-type granites. Hodgkinson Province.||||||
29977|Claret Creek Supersuite|23624|4|Described|p25|Late Carboniferous|Late Carboniferous|||||||14-JAN-09
29977|Claret Creek Supersuite|43060|4|Described|p100|||||||||
29977|Claret Creek Supersuite|44246|6|Mentioned|Map Legend||Late Carboniferous|||||||
29977|Claret Creek Supersuite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
29977|Claret Creek Supersuite|60425|3|Fully described|p41, p60 Tb. 4, p77, p282-3 Appdx.|Early Permian|Late Carboniferous|Incl:Claret Creek Suite+other comagmatic intrusive rocks of Claret Creek Ring Complex - Ballast Ck Dacite, Hammonds Ck (part?)+ Munderra Granodiorites, The Gorge Rhyolite, Three Mile Microgranite? Age: 300+/-5Ma, 290Ma (Rb-Sr). Lith.details incl. I-type||||||07-FEB-11
29977|Claret Creek Supersuite|62371|5|Briefly described|p472 Fig.3|Carboniferous|Carboniferous|||||||
29977|Claret Creek Supersuite|63140|6|Mentioned|p572 fig 3|Carboniferous|Carboniferous|||||||
29977|Claret Creek Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province.||||||
29977|Claret Creek Supersuite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Appears to be an alternative name for (or has superseded?) the Claret Creek Ring Complex.|||Includes Claret Creek Volcanics, Munderra Granodiorite, Three Mile Microgranite, The Gorge Rhyolite and Ballast Creek Dacite.|||
29977|Claret Creek Supersuite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Appears to be an alternative name for (or has superseded?) the Claret Creek Ring Complex.|||Includes Claret Creek Volcanics, Munderra Granodiorite, Three Mile Microgranite, The Gorge Rhyolite and Ballast Creek Dacite.|||
29977|Claret Creek Supersuite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province|||Includes Arra Granite, Bonnor Creek Granite.|Younger than White Springs Supersuite rocks.||
29977|Claret Creek Supersuite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit (in part), as well as the Almaden, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||
29977|Claret Creek Supersuite|69030|5|Briefly described|p6|Permian|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.|300 +/- 5 Ma (Rb/Sr isochron age).|||||
29977|Claret Creek Supersuite|69593|5|Briefly described|p484-486, p489, p502-506, p510|||Western Herberton and eastern Tate Subprovinces, Kennedy Igneous Association. Outcrop area ~250 km2. Geochemistry described.|||Claret Creek Suite; Claret Creek Volcanics; Hammonds Creek, Munderra, Mount Pudding Basin Granodiorites.||Hornblende-biotite granodiorite and tonalite,  biotite microgranite; includes associated rhyolitic volcanics and dacite ring dykes (Claret Creek Volcanics). I-type.|
27743|Claret Creek Volcanics|23423|4|Described|p309 Table 7.3||Late Carboniferous|Also see p236. Claret Creek Supersuite. Underlying unit Hodgkinson Formation (unconformable). Kennedy Igneous Province.||||||
27743|Claret Creek Volcanics|23502|5|Briefly described|Map Legend||Late Carboniferous|of Claret Creek Ring Complex, Claret Creek Supersuite.||||||
27743|Claret Creek Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. 91. I-Type.||||||
27743|Claret Creek Volcanics|23616|5|Briefly described|Table 3 p55||Late Carboniferous|Unconform. on Hodgkinson Fm; cut by many dykes/plutons (mainly Munderra Granodiorite & Three Mile Microgranite)/zones of intrusive breccia (all part of the Claret Ck Ring Complex), as well as by the Opah Granite. Thick: ~430 m.||||||30-AUG-04
27743|Claret Creek Volcanics|23624|4|Described|p26|Late Carboniferous|Late Carboniferous|Parent: Claret Creek Supersuite.||||||08-JUL-15
27743|Claret Creek Volcanics|29605|4|Described|p4|||||||||
27743|Claret Creek Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27743|Claret Creek Volcanics|31832|6|Mentioned|Table 6|||||||||
27743|Claret Creek Volcanics|36527|6|Mentioned|p160|||||||||
27743|Claret Creek Volcanics|37613|6|Mentioned|Fig.1|||||||||
27743|Claret Creek Volcanics|39445|5|Briefly described|Table 7|||||||||
27743|Claret Creek Volcanics|39831|6|Mentioned|p319|||||||||
27743|Claret Creek Volcanics|42547|5|Briefly described|p74|||||||||
27743|Claret Creek Volcanics|43259|4|Described|Appendix 1,p9.||Carboniferous|Rb-Sr age is 301 Ma.||||||
27743|Claret Creek Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
27743|Claret Creek Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27743|Claret Creek Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
27743|Claret Creek Volcanics|45014|14|Not recorded|p86-8,136,Pl.38,Tb.1|Late Carboniferous|Early Carboniferous|See base card. (Middle-Late Carboniferous)||||||
27743|Claret Creek Volcanics|45025|4|Described|p69-70|Permian|Carboniferous|||||||
27743|Claret Creek Volcanics|46845|6|Mentioned|Table 1|||||||||
27743|Claret Creek Volcanics|60425|4|Described|p40-41, p50 tb. 3|Late Carboniferous|Late Carboniferous|Of Claret Creek Supersuite. Comprises Ballast Creek Dacite and The Gorge Rhyolite. At margins of Claret Ck Ring Complex. Age: 300+/-5Ma (Rb-Sr). Thickness:~430m. Rhyolitic ignimbrite + intercalated lenses of volc.breccia, minor intrusive dacite, rhyodacite||||||01-JUL-15
27743|Claret Creek Volcanics|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Lithic-rich, welded, rhyolitic to rhyodacitic ignimbrite, volcanic breccia.|
27743|Claret Creek Volcanics|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Lithic-rich, welded, rhyolitic to rhyodacitic ignimbrite, volcanic breccia.|
27743|Claret Creek Volcanics|69593|6|Mentioned|p504|||||Claret Creek Supersuite.||||
25711|Clarke River Group|22800|5|Briefly described|Fig.14 p592||Famennian|||||||
25711|Clarke River Group|23032|4|Described|p17,34|Late Carboniferous|Devonian|||||||
25711|Clarke River Group|23423|5|Briefly described|Plate 8.3e|||||||||
25711|Clarke River Group|23424|4|Described|Table 8.1 Fig 8.2 p328 Fig 8.3/8.4 p337.||Visean|Age: Early Carboniferous (Visean); palynomorphs. Intruded by Carboniferous granites and rhyolite plugs overlain by Wade beds and tertiary basalt and sediments. Geological Province Clarke River Basin.||||||21-JUN-13
25711|Clarke River Group|23430|4|Described|p478, p508-509|||Clarke River Basin Province.||||||
25711|Clarke River Group|23431|5|Briefly described|p542|||||||||
25711|Clarke River Group|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
25711|Clarke River Group|23617|4|Described|p14|||The rocks have not been compared with Clarke River Group in EINASLEIGH and CLARKE RIVER, and have therefore been assigned to the group, rather than to a formation. Underlying unit Kangaroo Hills Formation. Camel Ck Subprovince of Broken River Province.||||||
25711|Clarke River Group|23618|5|Briefly described|map legend|Carboniferous|Devonian|||||||
25711|Clarke River Group|23619|5|Briefly described|p17|Tournaisian|Late Devonian|Underlying unit Kangaroo Hills Formation - unconformable.||||||
25711|Clarke River Group|23893|5|Briefly described|p9 Fig. 4|Early Permian|Late Carboniferous|||||||
25711|Clarke River Group|24577|5|Briefly described|p754 Fig. 2|Late Paleozoic|Late Paleozoic|Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||07-NOV-08
25711|Clarke River Group|24613|5|Briefly described|p6 Fig. 3, p94, p135|Early Carboniferous|Late Devonian|Includes Lyall and Venetia Formations. Geological province: Burdekin Basin.||||||21-JUN-13
25711|Clarke River Group|24614|5|Briefly described|p191 Fig. 1|||Includes the Lyall and Venetia Formations. Max. thickness: ~6000m. Geological Province: Clarke River Basin.||||||07-FEB-11
25711|Clarke River Group|40943|1|Redefined|p50|Late Carboniferous|Tournaisian|Tournaisian to Late Carboniferous. Previously Clarke River Formation||||||
25711|Clarke River Group|41260|3|Fully described|p22|||Originally Clarke River Formation||||||
25711|Clarke River Group|41679|6|Mentioned|Fig.1|||||||||
25711|Clarke River Group|41719|6|Mentioned|p217|||||||||
25711|Clarke River Group|41735|6|Mentioned|p284|||||||||
25711|Clarke River Group|41776|4|Described|p527|||||||||
25711|Clarke River Group|42031|5|Briefly described|Fig.4 P76i|||||||||
25711|Clarke River Group|42279|6|Mentioned|Fig.2 P18|||||||||
25711|Clarke River Group|42690|5|Briefly described|map legend|Carboniferous||||||||
25711|Clarke River Group|42692|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25711|Clarke River Group|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25711|Clarke River Group|42752|5|Briefly described|p48|||see also Fig.2 P46, Fig.3 P47||||||
25711|Clarke River Group|42933|1|Redefined|p203|Early Carboniferous|Late Devonian|||||||
25711|Clarke River Group|43095|5|Briefly described|Plate 2|||||||||
25711|Clarke River Group|43113|6|Mentioned|p33|||||||||
25711|Clarke River Group|43259|6|Mentioned|Appendix 1,p5.||Carboniferous|Early Carboniferous? in age.||||||
25711|Clarke River Group|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
25711|Clarke River Group|61727|5|Briefly described|p942 Fig.1|Early Carboniferous|Devonian|Overlies Kangaroo Hills Formation. Geological Province: Broken River Province/Camel Creek Subprovince. See also 943 Fig.2||||||
25711|Clarke River Group|63154|5|Briefly described|p281 Fig. 3|Early Carboniferous|Late Devonian|Geological province: Broken River Province/Camel Creek Subprovince. Includes small granites at ~357-322Ma.||||||11-APR-07
25711|Clarke River Group|67402|6|Mentioned|p244|||Clarke River Basin. |||Includes the Venetia, Ruxton and Lyall Formations.|||
25711|Clarke River Group|67848|5|Briefly described|p3 Fig.2.|Early Carboniferous|Late Devonian|Extensional cover succession over the collisional accretion succession. See also references to Clarke River Formation (pp13-14, p16).||||||
25711|Clarke River Group|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Venetia and Lyall Formations.|||
25711|Clarke River Group|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Venetia, Ruxton and Lyall Formations.|||
25711|Clarke River Group|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Venetia, Ruxton and Lyall Formations.|||
25711|Clarke River Group|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Venetia and Lyall Formations.|||
25711|Clarke River Group|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.|||Includes Ruxton Formation.|||
25711|Clarke River Group|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.|||Includes Ruxton Formation.|||
25711|Clarke River Group|68478|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Lyall Formation and Venetia Formation.||Fluvial and lacustrine and minor marine sedimentary and felsic volcanic rocks.|
25711|Clarke River Group|68479|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Clarke River Basin.|||Includes Lyall Formation and Venetia Formation.||Fluvial and lacustrine and minor marine sedimentary and felsic volcanic rocks.|
25711|Clarke River Group|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province.||||||
25711|Clarke River Group|68576|6|Mentioned|Q_11: p40|Early Carboniferous|Early Carboniferous|Includes an unnamed basal conglomerate containing clasts sourced from the Perry Creek and Kangaroo Hills Formations and Tribute Hills Arenite.||||||
25711|Clarke River Group|69030|5|Briefly described|p6, p15, p40|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province.|||Venetia, Ruxton, Lyall Formations.|||
25711|Clarke River Group|69079|6|Mentioned|p63|||Hosts sporadically-distributed antimony mineralisation in fissure veins, thoughout the Graveyard Creek Subprovince.||||||
25711|Clarke River Group|69592|5|Briefly described|p251 Fig.4.35, p258, p272, p274 Fig.4.65|Mississippian|Mississippian|See also p275, p278-279, p297. Clarke River Basin, Broken River Province. Has a marked basal angular unconformity with underlying Camel Creek Subprovince rocks. Up to 1300m thick. Deformation and its timing discussed.|||Ruxton, Venetia, Lyall Formations.|Unconformably overlies Kangaroo Hills Formation. Is overlain unconformably by Wade beds.||
25711|Clarke River Group|69593|6|Mentioned|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.|||Lyall Formation.|||
25711|Clarke River Group|70033|5|Briefly described|p5, p56|Visean||Clarke River Basin. Max age: late Famennian?||||||
25711|Clarke River Group|70207|6|Mentioned|p20|Carboniferous|Carboniferous|Clarke River and/or Cairns region.||||||
25711|Clarke River Group|73201|6|Mentioned|p610, p620|Mississippian|Late Devonian|Broken River Province. Pronounced angular unconformity with the older Broken River subduction complex. Generally disposed in gentle open folds. Oldest conodonts indicate an age close to the Famennian-Tournaisian boundary.||||||
40870|Clayhole Schist|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Of the Balcooma Metavolcanic Group.  Mica schist and quartzite.||||||
40870|Clayhole Schist|67455|6|Mentioned|p575 Table 1. |||||Unit in Balcooma Metavolcanic Group.||||
40870|Clayhole Schist|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Balcooma Metavolcanic Group.|||Mica schist and quartzite grading into gneiss.|
40870|Clayhole Schist|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Balcooma Metavolcanic Group.|||Mica schist and quartzite grading into gneiss.|
40870|Clayhole Schist|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.||Unit in Balcooma Metavolcanic Group.|||Mica schist and quartzite.|
40870|Clayhole Schist|68731|5|Briefly described|p152, p154 Fig 3.56, p157 Fig 3.63|Early Ordovician|Early Ordovician|Sedimentary structures are mainly planar laminae, but micro-cross-laminae and graded beds have been recognised. Detailed lithology discussed. Includes the Golden Creek Meta-andesite within its upper part.||Of the Balcooma Metavolcanic Group.|||Consists of interbedded mica schist and thin- to thick-bedded quartzite. Mica schist is fine- to medium-grained with quartz, muscovite, biotite, and some plagioclase.|
36503|Cleanskin Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 145.  I-Type.||||||
36447|Clearview Suite|23430|5|Briefly described|p480|Ordovician|Early Ordovician|469+/-12 Ma.||||||
36447|Clearview Suite|68731|5|Briefly described|p147|Middle Ordovician|Early Ordovician|Interpreted as a partial melt resulting from a high-grade metamorphic event in the Cape River Metamorphics. See also Clayhole Tuff Member.|469 +/- 12 Ma|||||
38223|Clearview Supersuite|23422|4|Described|p211 Table 6.7|||||||||
33152|Cleethorpes Granodiorite|60481|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Grey, medium grained hornblende biotite granodiorite.||||||
33152|Cleethorpes Granodiorite|61035|4|Described|p17 Tb. 2|Triassic|Permian|Inturdes Marlborough Metamorphics and Princhester Serpentinite. Age: 243+/-5Ma (isotopic age). Consists of Grey, medium-grained hornblende-biotite granodiorite.||||||07-FEB-11
33152|Cleethorpes Granodiorite|65388|2|Defined|p427-428, p70, 152, 153, 155, 156, 432|Early Triassic|Late Permian|Intrudes Marlborough Metamorphics, Princhester Serpentinite.  K-Ar dating gave minimum ages ranging from 235+/-5Ma to 243+/-5Ma (Webb & McDougall, 1968). Fresh, grey, medium-grained, equigranular hornblende-biotite granodiorite in type area. Weathered elsewhere.||||||
33152|Cleethorpes Granodiorite|68679|5|Briefly described|p308, p311, p410, p424, p426|Permian|Permian|Marlborough Province. A circular body ~10km in diameter, near Marlborough. Age determinations on 4 samples by Webb and McDougall (1968).|245 +/- 5 Ma to 235 +/- 5 Ma.|||Intrudes Princhester Serpentinite/Marlborough Metamorphics.|Hornblende-biotite granodiorite.|
33152|Cleethorpes Granodiorite|69952|6|Mentioned|p75|Early Triassic|Permian|||||||
23490|Clemant Microgranite|23422|5|Briefly described|p181, p205 Table 6.3|Early Carboniferous|Early Carboniferous|Of Oweenee Supersuite.||||||
23490|Clemant Microgranite|23423|5|Briefly described|p252||Carboniferous|Age: 337 +/- 6 Ma.||||||
23490|Clemant Microgranite|23497|6|Mentioned|p30|||of Bedarra belt. Age 337+/-6 Ma.||||||
23490|Clemant Microgranite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23490|Clemant Microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 133. Assumed to be I-Type.||||||
23490|Clemant Microgranite|23893|6|Mentioned|p18|Carboniferous|Carboniferous|Geological Province: Kennedy Province.||||||
23490|Clemant Microgranite|42689|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
23490|Clemant Microgranite|43095|2|Defined|p57|Early Carboniferous||Age is not certain.||||||
23490|Clemant Microgranite|43259|4|Described|Appendix 1,p24.|Permian|Carboniferous|||||||
23490|Clemant Microgranite|43589|2|Defined|p21||Early Carboniferous|Age: 337+/-7 Ma (U-Pb SHRIMP). Intrudes the Paluma Rhyolite, Saint Giles Volcanics, Holborn Granodiorite and the Argentine Metamorphics.  This microgranite forms ring dykes.||||||27-AUG-14
23490|Clemant Microgranite|60425|5|Briefly described|p98|Early Carboniferous|Early Carboniferous|Of the Oweenee Supersuite. Age: 337+/-6Ma.  I-type granite.||||||27-AUG-14
23490|Clemant Microgranite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Paluma Rhyolite.|Grey to pink, abundantly porphyritic biotite microgranite.|19-JUN-13
23490|Clemant Microgranite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Paluma Rhyolite.|Grey to pink, abundantly porphyritic biotite microgranite.|
23490|Clemant Microgranite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
41798|Clement Creek Quartz Monzodiorite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Grey, medium grained equigranular, biotite hornblende quartz monzodiorite; core of biotite granite.||||||
41798|Clement Creek Quartz Monzodiorite|61035|5|Briefly described|p10 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Broadsound and Clive Creek Volcanics. Equigranular, biotite-hornblende quartz monzodiorite; central core of medium-grained biotite granite containing K-feldspar megacrysts to 1cm. Geological Province: Connors Subprovince.||||||06-JUN-13
41798|Clement Creek Quartz Monzodiorite|65388|2|Defined|p355, p86, Fig. 35|Late Carboniferous|Late Carboniferous|Connors Arch pluton.  Intrudes and has hornfelsed Clive Creek Volcanics. Not dated, but probable age given. Mainly grey, fine to medium-grained biotite-hornblende quartz monzodiorite.||||||
41798|Clement Creek Quartz Monzodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus,Toobier, Tooloombah Creek and Waitara Granites; the Bora Creek Quartz Monzodiorite; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
41798|Clement Creek Quartz Monzodiorite|68679|6|Mentioned|p347|Carboniferous|Carboniferous|Northern New England Orogen.||||||
73797|Clements Creek beds|61035|6|Mentioned|p51|Permian|Permian|Informal name. Of the Lizzie Creek Volcanics. Acid volcanic rocks.||||||07-FEB-11
29611|Cliffdale Quarry Suite|43005|5|Briefly described|p215|||||||||
41800|Clive Creek Volcanics|60480|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Generally lithic rich, locally crystal rich rhyolitic to dacitic ignimbrite, minor cherty volcanic siltstone and well bedded rhyolitic tuff; rare quartzose sandstone.||||||29-SEP-04
41800|Clive Creek Volcanics|61035|5|Briefly described|p6|Carboniferous|Early Carboniferous|Of Connors Volcanic Group. Age: 350+/-7Ma (Withnall et al., 1998a,b; Hutton et al., 1999). Oldest unit in group. Lithic-rich rhyolitic ignimbrite, siltstone, sandstone, volcaniclastic arenites. Geol Prov: Connors Sudprovince.||||||07-FEB-11
41800|Clive Creek Volcanics|65388|4|Described|p85-89; p86, 88, 74, 94, 95, 104, 110|Early Carboniferous ||Of Connors Volcanic Group. Type area  in the upper reaches of Plumtree Creek. SHRIMP date of 348.9+/- 4 Ma. Unconformably overlain by the Broadsound Range Volcanics and Leura Volcanics. Intruded and hornfelsed by Camp Creek Granite, Clement Creek Quartz Monzodiorite. In faulted contact with Macksford Volcanics. See also p355, 360, 393.||||||04-SEP-14
41800|Clive Creek Volcanics|68679|4|Described|p353, p355, p356 Fig.5.40, p363|Tournaisian|Tournaisian|Southern Connors Subprovince. Occurs near the old Marlborough-Sarina road. Dating indicates a large hiatus before the overlying unit.|348.9 +/- 4.8 Ma (SHRIMP: Fanning et al., 2009).|Basal Connors Volcanic Group.||Is overlain by Broadsound Range Volcanics or, where absent, Leura Volcanics.|Mainly moderately to poorly sorted, lithic, felsic, volcaniclastic sandstone and siltstone with minor laminated siltstone, fine quartz-rich sandstone and ignimbrite (columnar jointed rhyolitic ignimbrite shown in Fig.5.40).|
41800|Clive Creek Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|349+/-4.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
33914|Cloncurry Supersuite|22465|5|Briefly described|p934|||||||||
33914|Cloncurry Supersuite|23920|5|Briefly described|p1068|||Geological Province: Eastern Fold Belt.||||||
33914|Cloncurry Supersuite|23967|4|Described|p1331|Mesoproterozoic|Mesoproterozoic|Age: 1500-1530Ma.||||||
33914|Cloncurry Supersuite|24256|6|Mentioned|p49|||Geological Province: Mount Isa Block.||||||
33914|Cloncurry Supersuite|65396|5|Briefly described|p55, p61, p360|||Defined by Pollard et al. (1996). Mount Isa Inlier. 59-74 wt% SiO2. The product of partial melting of a dioritic to tonalitic source.|||||Monzogranite to syenogranite.|
33914|Cloncurry Supersuite|73553|6|Mentioned|p200|Calymmian|Calymmian|Williams-Naraku Igneous Province. Defined by Pollard et al., (1996) and Pollard (1998). These granites were subsequently included into the Williams Supersuite by Budd et al., (2001).|1530-1500 Ma|||||
78917|Clondalkin Granite|65388|2|Defined|p363|Early Permian|Late Carboniferous|In contact with Strathdee and Carminya Granodiorites, but relationships uncertain. Unconformably overlain by Leura Volcanics. Age inferred.  Mainly pink to red, pale green, or brown to reddish brown (deeply weathered) medium to fine-grained, uneven-grained to slightly porphyritic, leucocratic biotite monzogranite.||||||
36172|Clotten Granodiorite|23506|5|Briefly described|Map Legend||Early Permian|of Almaden Supersuite.||||||
36172|Clotten Granodiorite|60425|4|Described|p282-3 Appdx.|Early Permian|Early Permian|Uanssigned. I-type. Age is probably Early Permian (?). Medium to dark grey, medium- to fine-grained granodiorite.||||||07-FEB-11
24855|Cobbold Metadolerite|22533|6|Mentioned|p55|||In Georgetown Region||||||
24855|Cobbold Metadolerite|23220|5|Briefly described|p10|||Geochemically similar to Dead Horse Metabasalt. of Forsayth Subprovince.||||||
24855|Cobbold Metadolerite|23291|3|Fully described|p30|Paleoproterozoic|Paleoproterozoic|Geological Province: Georgetown Region.||||||25-MAY-15
24855|Cobbold Metadolerite|23430|5|Briefly described|p451|||||||||
24855|Cobbold Metadolerite|23510|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24855|Cobbold Metadolerite|23616|5|Briefly described|p27|||Of Robertson River Subgroup of the Etheridge Group.||||||
24855|Cobbold Metadolerite|23619|4|Described|p43 Table 2||Proterozoic|Intrudes Einasleigh Metamorphics. Georgetown Province.||||||
24855|Cobbold Metadolerite|24485|3|Fully described|p13 Tb.1|Mesoproterozoic|Mesoproterozoic|Age: 1656 +/- 2Ma. Intruded by the Fig Tree Granite Complex, Nundah Granodiorite, McCord Granite and Carrs Granite. Geological Province: Etheridge Province||||||
24855|Cobbold Metadolerite|24486|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1650Ma. Geological Province: Forsayth Sub-province (Etheridge Province).||||||18-JUN-15
24855|Cobbold Metadolerite|37576|5|Briefly described|p8|||||||||
24855|Cobbold Metadolerite|38714|2|Defined|p189|Mesoproterozoic|Mesoproterozoic|Formerly Cobbold Dolerite.||||||
24855|Cobbold Metadolerite|39445|5|Briefly described|Table 2|||See also P45||||||
24855|Cobbold Metadolerite|39566|6|Mentioned|p60|||||||||
24855|Cobbold Metadolerite|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24855|Cobbold Metadolerite|39924|4|Described|p341|||||||||
24855|Cobbold Metadolerite|41272|5|Briefly described|M 1of1 H06|||See also M 1of1 H04||||||
24855|Cobbold Metadolerite|41675|6|Mentioned|p7|||||||||
24855|Cobbold Metadolerite|41975|5|Briefly described|p436|||||||||
24855|Cobbold Metadolerite|43060|6|Mentioned|p34|||of Robertson River Subgroup||||||
24855|Cobbold Metadolerite|43083|6|Mentioned|p27|||Geological province: Georgetown Province.||||||17-JUN-09
24855|Cobbold Metadolerite|43113|4|Described|Table 2 p28||Paleoproterozoic|||||||07-NOV-08
24855|Cobbold Metadolerite|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
24855|Cobbold Metadolerite|43664|4|Described|p44|||Intrudes Etheridge Group||||||
24855|Cobbold Metadolerite|43740|6|Mentioned|Fig.5,p45||Proterozoic|||||||
24855|Cobbold Metadolerite|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24855|Cobbold Metadolerite|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24855|Cobbold Metadolerite|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Intrudes the Robertson River Subgroup. Of the Etheridge Group.||||||18-JUN-15
24855|Cobbold Metadolerite|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Intrudes Bernecker Creek, Daniel Creek, Corbett and Lane Creek Formations and Dead Horse Metabasalt.||||||07-NOV-08
24855|Cobbold Metadolerite|50537|6|Mentioned|p2.5, Table 2.1|||Of thr Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||30-JUL-04
24855|Cobbold Metadolerite|50595|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Intrudes: Daniel Creek Formation, Corbett Formation, Lane Creek Formation.||||||18-JUN-15
24855|Cobbold Metadolerite|65887|4|Described|p39-53|Statherian|Statherian|Sills and lesser dykes intruding Robertson River Subgroup. Up to >500m thick. Emplacement probably occurred as two discrete magmatic pulses: after Dead Horse Metabasalt, and Lane Creek Formation. LA-ICPMS U-Pb zircon ages range 1719+/-27 Ma to 1628+/-13 Ma.||||||05-JUN-15
24855|Cobbold Metadolerite|66800|5|Briefly described|p928, p932.|||Emplaced in at least two pulses, about 20 My apart. Correlated with Einasleigh Metamorphics mafic rocks on basis of similar chemical composition. Ages U/Pb SHRIMP.|1674.9+/- 3.3 Ma and 1655.9 +/- 2.2 Ma.||||Mafic intrusives.|05-JUN-15
24855|Cobbold Metadolerite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Georgetown-Coen-Yambo Inliers. Emplacement of sills.|1662 +/- 32 Ma.|Lower Etheridge Group.||||
24855|Cobbold Metadolerite|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||||
24855|Cobbold Metadolerite|67430|6|Mentioned|p25|||||||||
24855|Cobbold Metadolerite|68352|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Low K, Th and U radiometric responses.||Unit in Etheridge Group.||Intrudes Robertson River Subgroup.|Metagabbro, metadolerite, orthoamphibolite.|
24855|Cobbold Metadolerite|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||||Intrudes Bernecker Creek Formation and Robertson River Subgroup.|Metagabbro and metadolerite grading into orthoamphibolite.|
24855|Cobbold Metadolerite|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Low K, Th and U radiometric responses.||||Intrudes Robertson River Subgroup.|Metagabbro and metadolerite grading into orthoamphibolite.|19-JUN-13
24855|Cobbold Metadolerite|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Low K, Th and U radiometric responses.||||Intrudes Robertson River Subgroup except Lane Creek Formation.|Metagabbro and metadolerite grading into orthoamphibolite, local mafic granulite.|
24855|Cobbold Metadolerite|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||~ 1650-1560 Ma|Of the Etheridge Group.||Intrudes Daniel Creek Formation, Dead Horse Metabasalt, Corbett Formation, Lane Creek Formation.|Metagabbro and metadolerite grading into orthoamphibolite.|
24855|Cobbold Metadolerite|68576|5|Briefly described|Q_11: p24, p27-28|||Georgetown area. The sills outline basin-and-dome structures. Intrusion was probably soon after deposition of the Lane Creek Formation as it does not extend into the conformably overlying units.|1655 +/- 5 Ma (Black et al., 1998).|||Intrudes Lane Creek Formation (Etheridge Group).|Metadolerite and metagabbro sills. Consists mainly of plagioclase (mostly recrystallised) and hornblende; not foliated.|
24855|Cobbold Metadolerite|69591|5|Briefly described|p61, p64-65, p82, p108|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Comagmatic with Dead Horse Metabasalt.|1656 +/- 2 Ma.|Etheridge Group.||Intrudes Bernecker Formation and Robertson River Subgroup.||
24855|Cobbold Metadolerite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1656+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro.|
24855|Cobbold Metadolerite|71799|4|Described|p153 tbl 1, p155 fig 4|||Ages included are SHRIMP and ICPMS dates [not specified which are which] that includes: 1675+/- 3 Ma-1656 +/- 2 Ma (sills and dykes), 1663 +/- 3 Ma (basaltic flows). Ages are derived from Baker et al, 2010; Black et al, 1998; Black et al, 2005; Neumann and Kositcin, 2011. Alteration is briefly mentioned. See also p156, p157 fig 5, p158.||||Overlain by the Townley Formation.|Low K tholeiitic metadolerite.|03-OCT-18
24855|Cobbold Metadolerite|72297|5|Briefly described|p712, p718|||About 30km SW of Georgetown.|||||Dolerite with pegmatite dykes containing lithium (in lepidolite and amblygonite) with tantalite, cassiterite and ilmenite, adjacent to greisenised granite.|
24855|Cobbold Metadolerite|73642|5|Briefly described|p10 Fig.8|Statherian|Statherian||1656+/-4 Ma|||||
24855|Cobbold Metadolerite|75079|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier.|c.1665 Ma.|||Intrudes Etheridge Group.||
41789|Cobweb Mountain Rhyolite|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Felsic volcaniclastic sandstone, conglomerate, breccia and siltstone (tuff?); minor rhyolite flows.||||||17-SEP-04
41789|Cobweb Mountain Rhyolite|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Felsic volcanoclastic sandstone, conglomerate, breccia and siltstone; minor rhyolite flows.||||||29-SEP-04
41789|Cobweb Mountain Rhyolite|61035|4|Described|p7|Early Permian|Late Carboniferous|Of the Lizzie Creek Volcanic Group. In Croydon area, overlain by Mount Benmore Volcanics. Lithology; felsic volcaniclastic sandstone, conglomerate, breccia + sitlstone + minor rhyolite flows. Geological Province: Connors Sudprovince.||||||07-FEB-11
41789|Cobweb Mountain Rhyolite|65388|4|Described|p115-117; p116 Fig.47, p85, 86, 110, 124|Early Permian||Of Lizzie Creek Volcanic Group. The type section (~200m thick) is designated at Cobweb Mountain between MGA 727750 7513900 (the basal conglomerate overlying the Leura Volcanics conformably) and MGA 727900 7512950, where it is overlain by basalt of the Mount Benmore Volcanics conformably;||||||
41789|Cobweb Mountain Rhyolite|68679|5|Briefly described|p355, p357-360|||Connors Subprovince. Crops out SE of Croydon homestead and W of Killarney homestead. At Cobweb Mountains the basal conglomerate contains well-rounded clasts of underlying Leura Volcanics.||Lizzie Creek Volcanic Group.||Overlies Leura Volcanics. Is overlain by Mount Benmore Volcanics.|Very thick basal pebble to boulder conglomerate; volcanic sandstone and poorly sorted granule to pebble conglomerate; some poorly sorted sandstone and siltstone; strongly flow-banded, feldspar-phyric rhyolite (?flow); rhyolitic breccia.|
36611|Cockatoo Spring granite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36611|Cockatoo Spring granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 412.  I-Type.||||||
24856|Cockie Spring Tonalite|23291|4|Described|p89 Fig. 3.8|Ordovician|Ordovician|See also Cockie Springs Tonalite. Intrudes Balcooma Metavolcanics and Lugano Metavolcanics. Intruded by Dido Tonalite (Dido Supersuite - Silurian). Geological Province: Georgetown Region.||||||08-JUL-15
24856|Cockie Spring Tonalite|23431|6|Mentioned|p532|||||||||
24856|Cockie Spring Tonalite|23619|4|Described|p42 Table 2|||Intrudes Lugano Metamorphics. Also see p7. Georgetown Province.||||||30-APR-15
24856|Cockie Spring Tonalite|41675|2|Defined|p59|Early Paleozoic||||||||07-NOV-08
24856|Cockie Spring Tonalite|42054|6|Mentioned|p272|||||||||
24856|Cockie Spring Tonalite|42279|6|Mentioned|Fig.2 P18|||||||||
24856|Cockie Spring Tonalite|42692|5|Briefly described|map legend|Ordovician||||||||
24856|Cockie Spring Tonalite|43113|4|Described|Table 2 p27|||Probably Early Palaeozoic (Ordovician?)||||||
24856|Cockie Spring Tonalite|43253|5|Briefly described|map legend|Ordovician|Cambrian|||||||
24856|Cockie Spring Tonalite|43259|4|Described|Appendix 1,p20.||Ordovician|Ordovician?||||||
24856|Cockie Spring Tonalite|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Strongly foliated hornblende-biotite tonalite and tonalitic gneiss.||||||
24856|Cockie Spring Tonalite|67455|5|Briefly described|p575 Table 1, p576 Fig.2, p584 Fig.7. |||Lucky Creek domain, Greenvale Province. Intensely foliated.|||||Hornblende- and biotite-bearing tonalite with minor amphibolite.|
24856|Cockie Spring Tonalite|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.|||||Strongly foliated hornblende-biotite tonalite and tonalitic gneiss.|
24856|Cockie Spring Tonalite|68731|5|Briefly described|p153 Fig 3.52, p153 Fig 3.53, p155, p158|Early Ordovician|Early Ordovician|Foliation is defined by elongate quartz and phyllosilicates; typically steeply dipping and trending to the northeast.||||Intrudes the central part of the Lugano Metamorphics.|Comprises strongly foliated hornblende-biotite tonalite containing abundant mafic xenoliths, and dykes of amphibolite and gneissic leucogranite.|03-JUL-14
37963|Cockroach Group|61404|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Includes the Tomahawk and Ninmaroo Formations.  Geological Province: southern Georgina Basin.||||||12-OCT-05
37963|Cockroach Group|62983|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|Carbonate platform deposition. Geological Province: Georgina Basin. Written in informal format as Cockroach group.||||||23-JAN-07
37963|Cockroach Group|64068|2|Defined|p225-226, pp70-75, p7, 38, p ix|Early Ordovician|Late Cambrian|New name. Top of Group is diachronous: Late Cambrian in west to Early Ordovician in east.|||Includes Chatsworth Limestone, Ninmaroo, Tomahawk and Swift Formations.|Overlies various units of Narpa Group. Is overlain by Kelly Creek Formation.||21-MAR-16
37963|Cockroach Group|65341|6|Mentioned|pp18-19.||||||Includes Tomahawk Formation.|||
37963|Cockroach Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.||||||Includes Chatsworth Limestone, Gola beds, Ninmaroo Formation, Swift Formation|||
37963|Cockroach Group|67870|5|Briefly described|p43, p47, p50-53|Ordovician|Late Cambrian|Georgina Basin. Potential hydrocarbon reservoir.|||Tomahawk Formation, Chatsworth Limestone.||Organic-rich (1-2% TOC) limestone, ooid limestone, shaly limestone, organic-rich siltstone; minor sandstone.|
37963|Cockroach Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Ordovician|Cambrian|Georgina Basin. ||||||
37963|Cockroach Group|69377|5|Briefly described|map legend|Early Ordovician|Cambrian||||Ninmaroo Formation, Chatsworth Limestone|||
37963|Cockroach Group|69443|5|Briefly described|p28:3, 5, 7, 16, 25-27|Early Ordovician|Late Cambrian|Kruse in Dunster et al. (2007). Southern Georgina Basin. Widely distributed. The upper extent of this unit is diachronous. Is correlated with Pacoota Sandstone and ?Djagamara Formation.|||Chatsworth Limestone; Tomahawk, Ninmaroo, Swift Formations.|Overlies Narpa Group units conformably or disconformably. Is overlain conformably (locally disconformably) by Kelly Creek Formation (Toko Group).||12-JUL-16
37963|Cockroach Group|69591|5|Briefly described|p29, p91, p93-94|Early Ordovician|Cambrian|The carbonate-dominated Kelly Creek Formation and Coolibah Formation are here added to this Group, transferred from the otherwise clastic-dominated Toko Group.|||Ninmaroo, Swift, Kelly Creek, Coolibah Formations.||Predominantly carbonates.|
37963|Cockroach Group|69673|6|Mentioned|p111, p114 fig 92, p117||||||Includes Tomahawk Formation, Ninmaroo Formation, Swift Formation|||
37963|Cockroach Group|70749|5|Briefly described|p54|||Georgina Basin, Centralian Superbasin.|||Tomahawk, Ninmaroo Formations.|||
37963|Cockroach Group|72321|6|Mentioned|Fig 2||Jiangshanian|Burke River Structural Belt, Georgina Basin. |||Includes Chatsworth Limestone.|||
37963|Cockroach Group|72515|5|Briefly described|Map Legend|Ordovician|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Includes trilobite and rostroconchs fossils.|||Includes the Tomahawk Formation.|Unconformably overlain by the Alcoota beds. disconformably overlies the Narpa Group.||
37963|Cockroach Group|72516|5|Briefly described|p11, p21, p85, p94, p135, p171, p176|Ordovician|Furongian|Georgina Basin.|ca. 500 Ma (Maximum depositional age)||Includes the Tomahawk Formation.|||
37963|Cockroach Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
37963|Cockroach Group|73137|6|Mentioned|p6|Early Ordovician|Cambrian|||||||
37963|Cockroach Group|73553|6|Mentioned|p7|Early Ordovician|Cambrian|||||||
27128|Coffin Hill Member|9528|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Clayey lithic quartzose sandstone, commonly ferruginous and/or glauconitic; mottle purple siltstone.; pebbly in places.||||||
27128|Coffin Hill Member|9531|5|Briefly described|Map  Legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, siltstone, shale/claystone.||||||02-JUL-04
27128|Coffin Hill Member|23032|5|Briefly described|p47|Cretaceous||||||||
27128|Coffin Hill Member|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Parent: Gilbert River Fromation. Geological Province: Georgetown Region.||||||08-JUL-15
27128|Coffin Hill Member|23425|4|Described|Table 9.7 p394.|||Of Gilbert River Formation.  Carpentaria Basin Province.||||||
27128|Coffin Hill Member|23496|5|Briefly described|Table 4, p59|Aptian|Neocomian|of Smart and Others 1971. of Gilbert River Formation. ~37m thick.||||||
27128|Coffin Hill Member|23500|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of Gilbert River Formation, Carpentaria and Karumba Basins. Age shown as Late Jurassic? - Early Cretaceous.||||||
27128|Coffin Hill Member|23510|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|of Gilbert River Formation.||||||
27128|Coffin Hill Member|23616|5|Briefly described|Table 1C p12|Early Cretaceous|Late Jurassic|Unconformably overlies Proterozoic metamorphics and granitoids of the Dargalong Inlier, Silurian granitoids of the Blackman Gap Supersuite, & Carboniferous granitoids & felsic volcanics of Scardons Volcanic Gp. Of Gilbert Rvr Fm. Yappar Mbr.||||||19-JUN-13
27128|Coffin Hill Member|23713|5|Briefly described|p76 Appendix 2.|||Of Gilbert River Formation.||||||
27128|Coffin Hill Member|24073|5|Briefly described|p378 Table 2|||Of the Gilbert River Formation.  Maximum thickness: 60m.  Geological Province: Carpentaria Basin.||||||
27128|Coffin Hill Member|24485|3|Fully described|p37, p38 Tb.6|Aptian|Neocomian|Underlying Unit: Yappar Member. Parent: Gilbert River Formation. Max Thickness: ~37m. Geological Province: Carpentaria Basin||||||
27128|Coffin Hill Member|24486|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Geological Province: Carpentaria Basin.||||||
27128|Coffin Hill Member|30020|6|Mentioned|p29|||||||||
27128|Coffin Hill Member|30584|4|Described|Table 1|||||||||
27128|Coffin Hill Member|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
27128|Coffin Hill Member|31168|5|Briefly described|p11|||Also on Table 2.||||||
27128|Coffin Hill Member|32314|6|Mentioned|Fig. 4|||||||||
27128|Coffin Hill Member|33176|6|Mentioned|p172|||Refers identification||||||
27128|Coffin Hill Member|33179|4|Described|Table 2|||||||||
27128|Coffin Hill Member|33180|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
27128|Coffin Hill Member|33182|5|Briefly described|p190|||Lower Cretaceous||||||
27128|Coffin Hill Member|33183|2|Defined|p233|early Aptian|early Aptian|Gilbert R. Fm.||||||
27128|Coffin Hill Member|33528|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
27128|Coffin Hill Member|35220|6|Mentioned|p16|||||||||
27128|Coffin Hill Member|35811|5|Briefly described|p563|||||||||
27128|Coffin Hill Member|37608|3|Fully described|Table 2|||||||||
27128|Coffin Hill Member|39211|5|Briefly described|p36|||See Fig. 22||||||
27128|Coffin Hill Member|39917|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Early Cretaceous||||||
27128|Coffin Hill Member|40218|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
27128|Coffin Hill Member|41064|6|Mentioned|Fig.5|||||||||
27128|Coffin Hill Member|41361|6|Mentioned|Fig.3|||||||||
27128|Coffin Hill Member|42061|4|Described|p153|||||||||
27128|Coffin Hill Member|42369|5|Briefly described|Fig.10, P61|||Member of Gilbert River Formation||||||
27128|Coffin Hill Member|42691|5|Briefly described|map legend|Mesozoic||||||||
27128|Coffin Hill Member|42933|5|Briefly described|p236|||of Gilbert River Formation||||||
27128|Coffin Hill Member|43060|5|Briefly described|p59,Table 1c|||of Gilbert River Formation||||||
27128|Coffin Hill Member|43110|5|Briefly described|p54|||of Gilbert River Formation||||||
27128|Coffin Hill Member|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|of Gilbert River Formation||||||
27128|Coffin Hill Member|43287|5|Briefly described|Map Legend||Mesozoic|of Gilbert River Formation. Late Jurassic? to Early Cretaceous.||||||
27128|Coffin Hill Member|43603|5|Briefly described|p9|||||||||
27128|Coffin Hill Member|43625|6|Mentioned|p48|||||||||
27128|Coffin Hill Member|44246|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
27128|Coffin Hill Member|44926|5|Briefly described|Map Legend|||Late Jurassic? - Early Cretaceous||||||
27128|Coffin Hill Member|45145|3|Fully described|Table 5|||||||||
27128|Coffin Hill Member|50198|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.||||||
27128|Coffin Hill Member|50199|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.||||||
27128|Coffin Hill Member|50210|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Overlies: Yappar Member.||||||
27128|Coffin Hill Member|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Of the Gilbert River Formation. Overlies: Yappar Member.||||||01-JUL-04
27128|Coffin Hill Member|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Gilbert River Formation (Eulo Queen Group). Fine to coarse clayey lithic-quartzose sandstone.  Overlies Yappar Member in same formation.||||||06-JUL-04
27128|Coffin Hill Member|60081|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Clayey sandstone, siltstone, some shale, locally glauconitic at top; fossiliferous.||||||
27128|Coffin Hill Member|60087|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Glauconitic quartzose sandstone, shale.||||||
27128|Coffin Hill Member|60357|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation. Underlies: Wallumbilla Formation. Overlies: Yappar Member. Geological Province: Carpentaria Basin.||||||20-AUG-04
27128|Coffin Hill Member|62837|5|Briefly described|Stratigraphic columns|Valanginian|Valanginian|Of the Gilbert River Formation. Age: ~129-~123Ma. Geological Province: Burketown Depression.||||||
27128|Coffin Hill Member|67402|6|Mentioned|p180|||||Gilbert River Formation||||
27128|Coffin Hill Member|68345|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Unit in Gilbert River Formation.||Overlies Yappar Member conformably. Is overlain conformably by Wallumbilla Formation.|Medium- to coarse-grained clayey quartzose sandstone, pebbly sandstone, minor quartz-pebble conglomerate, siltstone, fine quartzose sandstone, mudstone; ferruginised in places; commonly bioturbated.|
27128|Coffin Hill Member|68349|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Unit in Gilbert River Formation.||Conformably overlies Yappar Member. Is overlain conformably by Wallumbilla Formation.|Medium- to coarse-grained clayey quartzose sandstone, pebbly sandstone, minor quartz-pebble conglomerate, siltstone, fine quartzose sandstone, mudstone; ferruginised in places; commonly bioturbated.|
27128|Coffin Hill Member|68356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Upper unit in Gilbert River Formation.||Conformably overlies Yappar Member.|Medium- to coarse-grained clayey quartzose sandstone, pebbly sandstone, minor quartz-pebble conglomerate, siltstone, fine quartzose sandstone, mudstone; ferruginised in places; commonly bioturbated.|
27128|Coffin Hill Member|68405|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins.||Of Gilbert River Formation.||Overlies Yappar Member.|Medium to coarse-grained, clayey quartzose sandstone, pebbly sandstone, minor quartz pebble conglomerate, siltstone, fine quartzose sandstone, mudstone; ferruginised in places.|24-AUG-15
27128|Coffin Hill Member|68417|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Of the Gilbert River Formation.||Conformably overlain by the Wallumbilla Formation. Conformably underlain by the Yappar Member.|Medium to coarse-grained clayey quartzose sandstone, pebbly sandstone, minor quartz-pebble conglomerate, siltstone, fine quartzose sandstone, mudstone; ferruginised in places; commonly bioturbated.|
27128|Coffin Hill Member|69594|5|Briefly described|p521, p540|Aptian|Early Cretaceous|Carpentaria Basin. Fluvial to marine deposition.||Gilbert River Formation.||Overlies Yappar Member. Equivalent to upper Gilbert River Formation.||
28099|Coleman River Gneiss|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
28099|Coleman River Gneiss|22781|4|Described|p18|Proterozoic|Proterozoic|Holroyd Group||||||
28099|Coleman River Gneiss|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group. Maybe high grade Dinah Formation||||||12-JAN-05
28099|Coleman River Gneiss|69591|5|Briefly described|p79 Tb.2.6|||Savannah Province, Coen Inlier. May be high-grade Dinah Formation. Occurs 10km east of Glengarland, small area on Coleman River.||Holroyd Group.|||Sillimanite-andalusite-mica-feldspar gneiss.|
27129|Colinlea Sandstone|13516|5|Briefly described|p145 fig 3, p147 fig 5|Late Permian|Late Permian|From western margin, Bowen Basin, Galilee Basin. Age: APP4 - APP5||||||
27129|Colinlea Sandstone|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
27129|Colinlea Sandstone|24071|5|Briefly described|p318|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
27129|Colinlea Sandstone|29411|5|Briefly described|p201|||||||||
27129|Colinlea Sandstone|29721|6|Mentioned|p65|||||||||
27129|Colinlea Sandstone|30102|6|Mentioned|p9|||||||||
27129|Colinlea Sandstone|30508|6|Mentioned|p91|||Reservoir potential. Stratigraphic drilling||||||
27129|Colinlea Sandstone|30691|4|Described|p6|||See also P14,20-22,Table 3,6. Permian age||||||
27129|Colinlea Sandstone|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27129|Colinlea Sandstone|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
27129|Colinlea Sandstone|30916|6|Mentioned|p99|||||||||
27129|Colinlea Sandstone|31120|4|Described|p151|||||||||
27129|Colinlea Sandstone|31121|6|Mentioned|p388|||||||||
27129|Colinlea Sandstone|31122|6|Mentioned|p344|||Overlies Joe Joe Group||||||
27129|Colinlea Sandstone|31258|6|Mentioned|p98|||||||||
27129|Colinlea Sandstone|31260|6|Mentioned|p16|||Refers facies analysis||||||
27129|Colinlea Sandstone|32493|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|32577|5|Briefly described|p23|||||||||
27129|Colinlea Sandstone|32639|6|Mentioned|p76|||||||||
27129|Colinlea Sandstone|33078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33079|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33086|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33092|5|Briefly described|p7|||Strat. table||||||
27129|Colinlea Sandstone|33096|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|33366|6|Mentioned|Fig.3|||Perm.||||||
27129|Colinlea Sandstone|33368|6|Mentioned|p213|||Strat. succession GSQ Jericho 1.||||||
27129|Colinlea Sandstone|33369|6|Mentioned|p213|||Strat. succession in GSQ Jericho 1||||||
27129|Colinlea Sandstone|33372|5|Briefly described|p22|||Correlative described from wells.||||||
27129|Colinlea Sandstone|33639|6|Mentioned|Fig.1|||See also P10.||||||
27129|Colinlea Sandstone|33640|6|Mentioned|Table 4|||||||||
27129|Colinlea Sandstone|33646|6|Mentioned|p10|||Palynological stage.||||||
27129|Colinlea Sandstone|33648|6|Mentioned|p17|||Palynological divisions||||||
27129|Colinlea Sandstone|33674|6|Mentioned|Fig.1|||||||||
27129|Colinlea Sandstone|33675|4|Described|p411|||Lithology.||||||
27129|Colinlea Sandstone|34132|6|Mentioned|p5|||Upper Permian||||||
27129|Colinlea Sandstone|34138|6|Mentioned|Cor.Chart|||Artinskian - Kungurian||||||
27129|Colinlea Sandstone|34174|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|34390|4|Described|Table 2|||Permian. Gebbie Subgroup.||||||
27129|Colinlea Sandstone|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|35457|4|Described|p629|||Also Fig.4 biostratigraphic relationships.||||||
27129|Colinlea Sandstone|35562|6|Mentioned|Table 5|||Biostratigraphy||||||
27129|Colinlea Sandstone|35845|6|Mentioned|p73|||See also Fig.25||||||
27129|Colinlea Sandstone|35937|6|Mentioned|p621|||||||||
27129|Colinlea Sandstone|36243|6|Mentioned|Table 3A|||||||||
27129|Colinlea Sandstone|36739|6|Mentioned|p21|||||||||
27129|Colinlea Sandstone|36921|4|Described|p184|||See also Table 1.||||||
27129|Colinlea Sandstone|37096|6|Mentioned|p248|||||||||
27129|Colinlea Sandstone|37451|6|Mentioned|Table 2|||||||||
27129|Colinlea Sandstone|37610|4|Described|p302|||||||||
27129|Colinlea Sandstone|39252|5|Briefly described|p20|||||||||
27129|Colinlea Sandstone|39261|6|Mentioned|Fig. 9|||||||||
27129|Colinlea Sandstone|39264|6|Mentioned|Fig. 13|||||||||
27129|Colinlea Sandstone|39445|5|Briefly described|Table 8|||||||||
27129|Colinlea Sandstone|39478|6|Mentioned|Table 1|||||||||
27129|Colinlea Sandstone|39754|6|Mentioned|p1690|||||||||
27129|Colinlea Sandstone|39942|6|Mentioned|p465|||||||||
27129|Colinlea Sandstone|39943|6|Mentioned|Table 5A|||||||||
27129|Colinlea Sandstone|40123|6|Mentioned|p465|||||||||
27129|Colinlea Sandstone|40623|5|Briefly described|p110|||||||||
27129|Colinlea Sandstone|41097|6|Mentioned|p165|||||||||
27129|Colinlea Sandstone|41116|4|Described|p433|||Briefly described Table 1||||||
27129|Colinlea Sandstone|41246|6|Mentioned|Map legend|Permian||||||||
27129|Colinlea Sandstone|41707|6|Mentioned|Fig.8|||||||||
27129|Colinlea Sandstone|41710|6|Mentioned|p222|||See also Fig.2||||||
27129|Colinlea Sandstone|42250|6|Mentioned|Fig.3 P30|||||||||
27129|Colinlea Sandstone|42256|6|Mentioned|Fig.1 P243|||||||||
27129|Colinlea Sandstone|42446|6|Mentioned|p1|||||||||
27129|Colinlea Sandstone|42447|6|Mentioned|Fig. 2|||||||||
27129|Colinlea Sandstone|42614|5|Briefly described|p14|||Galilee Basin||||||
27129|Colinlea Sandstone|42641|5|Briefly described|p108|||||||||
27129|Colinlea Sandstone|42856|6|Mentioned|p643|||||||||
27129|Colinlea Sandstone|42999|5|Briefly described|Table 1,p90|Late Permian|Late Permian|||||||21-DEC-11
27129|Colinlea Sandstone|43105|5|Briefly described|p13|||||||||
27129|Colinlea Sandstone|43114|6|Mentioned|Table 2|||||||||
27129|Colinlea Sandstone|43204|5|Briefly described|Map Legend|Late Permian|Late Permian|in the Denison Trough||||interfingers with Aldebaran Sandstone in part||23-DEC-11
27129|Colinlea Sandstone|43213|5|Briefly described|p10, p69, p154|Permian|Permian|Mollan et al. (1969). Crops out along the W flank of Denison Trough, across the Springsure Shelf, and along E flank of Galilee Basin. Correlated with upper Aldebaran Sandstone-Catherine Sandstone interval.|||||Fine- to medium-grained quartz sandstone and granule to cobble conglomerate, grading to pebbly sandstone.|
27129|Colinlea Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
27129|Colinlea Sandstone|43987|14|Not recorded|p267,270,278|||||||||
27129|Colinlea Sandstone|43994|14|Not recorded|Map Legend|||||||||
27129|Colinlea Sandstone|44172|14|Not recorded|Fig.1,T.1,p1332,1343|Kungurian|Artinskian|Equivalent to Catherine Sandstone, Freitag Formation and Ingelara Formation. Denison Trough||||||
27129|Colinlea Sandstone|44173|14|Not recorded|p11,112|||Basal part may be partly equivalent to Freitag Formation.||||||
27129|Colinlea Sandstone|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
27129|Colinlea Sandstone|44424|14|Not recorded|p293-301|||Represents Gebbie Subgroup on Springsure Shelf.||||||
27129|Colinlea Sandstone|44697|14|Not recorded|p91|||||||||
27129|Colinlea Sandstone|44700|14|Not recorded|p108|||Jericho No.1 well.||||||
27129|Colinlea Sandstone|45071|6|Mentioned|p32|||||||||
27129|Colinlea Sandstone|45073|5|Briefly described|p42|||Stratigraphy P58||||||
27129|Colinlea Sandstone|46849|6|Mentioned|Fig. 7|||||||||
27129|Colinlea Sandstone|48626|14|Not recorded|p22|||||||||
27129|Colinlea Sandstone|48900|2|Defined|p32|Early Permian|Early Permian|||||||
27129|Colinlea Sandstone|48920|3|Fully described|p23|||Permian age||||||
27129|Colinlea Sandstone|63713|5|Briefly described|p1507-1508, p1523, p1528|Wordian|Roadian|Eastern margin, Galilee Basin. Predominantly fluvial. On the E edge of the Springsure Shelf, this unit's name refers collectively to the upper Aldebaran Sandstone, Freitag and Ingelara Formations, and Catherine Sandstone. Well-log correlation.||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|63832|6|Mentioned|p131 fig 2|Guadalupian|Guadalupian|Of Galilee Basin.||||||
27129|Colinlea Sandstone|64288|5|Briefly described|p532 Fig.1 |Wordian|Kungurian|||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|64631|5|Briefly described|p44 Fig.2.|Wordian|Roadian|Galilee Basin. Biostratigraphic age control for base and top.||||Is overlain by Peawaddy Formation.||
27129|Colinlea Sandstone|64665|6|Mentioned|p53 Fig.2.|Late Permian|Middle Permian|Galilee Basin. Equivalent to Catherine Sandstone.||||||
27129|Colinlea Sandstone|65113|5|Briefly described|p349||Late Permian|Basal part of thin succession in Galilee Basin, west of Denision Trough. Equivalent to upper Aldebaran Sandstone. Whole succession continues up to Middle Triassic, but how much of this is Colinlea Sanstone is unclear.||||||
27129|Colinlea Sandstone|66188|6|Mentioned|431, Fig 3|Early Triassic|Late Permian|||||||
27129|Colinlea Sandstone|67323|5|Briefly described|p84|Permian|Permian|Eastern Galilee Basin.||||Correlated with Betts Creek beds.||
27129|Colinlea Sandstone|67402|4|Described|p43 tbl HPB1, p124 fig GLL1|Capitanian|Roadian|Galilee Basin. Highly prospective reservoir unit for the storage of carbon dioxide; has an estimated theoretical storage capacity of 1320 Megatonnes of carbon dioxide. At least 64m thick in the Galilee Basin. See also p125, p131 fig GLL12, p132, p134 fig GLL17, p135, p136, p141, p144, p305.||||Unconformably overlies the Jochmus Formation. Overlain by the Bandanna Formation.|Medium to coarse-grained quartzose sandstones interbedded with mudstones, siltstones and fine-grained tight sandstones.|
27129|Colinlea Sandstone|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-9, p16 Tb.4, p18-19|Lopingian|Guadalupian|Galilee Basin. Fluvial unit. Significant concentration of pyrite suggests prolonged marine influence. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Is overlain by Peawaddy Formation.|Light grey to brown, thick-bedded, fine- to coarse-grained, moderately to poorly sorted, sublabile to quartzose sandstone, conglomeratic in places; minor mudstone, siltstone and coal.|
27129|Colinlea Sandstone|68326|5|Briefly described|Map legend.|Permian|Permian|Galilee Basin.|||||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|02-DEC-13
27129|Colinlea Sandstone|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||Of the Back Creek Group.||Conformably underlain by the Reids Dome beds. Conformably overlain by the Peawaddy Formation.|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||Of the Back Creek Group.||Conformably overlain by the Peawaddy Formation. Underlain by the Joe Joe Goup.|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|18-JUN-13
27129|Colinlea Sandstone|68423|5|Briefly described|map legend|Permian|Permian|Galilee Basin.|||||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|68679|5|Briefly described|p378, p380|||Mollan et al. (1969). Bowen, Galilee Basins. 200m thick. Fluvial plain, marginal marine deposits.|||||Sandstone, pebbly sandstone, conglomerate.|
27129|Colinlea Sandstone|68731|6|Mentioned|p201 Fig 3.110|Lopingian|Lopingian|Correlative of the upper Aldebaran Sandstone, Feitag Formation, Ingelara Formation and Catherine Sandstone.||||||
27129|Colinlea Sandstone|69379|5|Briefly described|map legend|Permian|Permian|||Of Back Creek Group|||Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone|
27129|Colinlea Sandstone|69582|6|Mentioned|p66|||Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Aramac Coal Measures. Overlain by the Bandanna Formation.|Sandstone.|
27129|Colinlea Sandstone|70857|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group||Overlain by Peawaddy Formation|Quartz sandstone, pebbly quartz sandstone, minor conglomerate and siltstone.|
27129|Colinlea Sandstone|71265|5|Briefly described|p587, p589-592, p595-600, p603-607|Changhsingian|Wuchiapingian|Galilee Basin. References to "Colinlea Sandstone equivalent" as previously Colinlea Sandstone. 40-70m thick. Sedimentary logs of GSQ Muttaburra 1, CRD Montani 1 and OEC Glue Pot Creek 1. Facies discussed.||||Overlies Jochmus Formation (Joe Joe Group). Is overlain by Fair Hill Formation and Fort Cooper Coal Measures. Interfingers with, and lateral equivalent of, Peawaddy Formation.|Dominated by quartz-rich sandstone. Contains a series of fining-upward sequences capped by coal.|
27129|Colinlea Sandstone|71276|4|Described|p284-286, p288-295, p297-298|Lopingian|Lopingian|Mollan et al. (1969). Formerly the Colinlea Formation of Schneeberger (1952). Type section on the Springsure Shelf. Similar basal conglomerate, sandstone composition, and palynology to Betts Creek beds, but separation of > 450km makes correlation questionable. Suggested (Mollan et al., 1969) as probable lateral equivalent of Aldebaran Sandstone, Ingelara Formation and Catherine Sandstone. Coal seam correlation. Proposed in this study that, within the Galilee Basin, this unit be given the informal name "Colinlea Sandstone equivalent" on the grounds that the original description is no longer appropriate.||||Is overlain by Peawaddy Formation. Correlative of Betts Creek beds.|Predominantly fine to medium quartz sandstone with a kaolinitic matrix. Basal conglomerate. Contains four coal seams.|
27129|Colinlea Sandstone|71701|5|Briefly described|p155-p158, p163, p166-p169|Changhsingian|Changhsingian|Eastern Area and Springsure Shelf, Galilee Basin. Palynology of an equivalent unit is discussed briefly. ||||Overlies the Joe Joe Group. Overlain by the Fair Hill Formation. Equivalent to the upper part of the Moranbah Coal Measures.||
27129|Colinlea Sandstone|71710|5|Briefly described|p367, 370, p380-381, p386|||Southern Galilee Basin. ||||Equivalent to lower part of Betts Creek beds. Disconformity at base.||
27129|Colinlea Sandstone|72088|5|Briefly described|p8, p16, p18, p20-p21|Wuchiapingian|Wuchiapingian|Southern Galilee Basin. See also p38-p40, p43-p44, p68-p69, p91.||||Overlain by the Peawaddy Formation and the Bandanna Formation.||
27129|Colinlea Sandstone|72297|5|Briefly described|p752-753, p755|Permian|Permian|Galilee Basin. 120m thick. Hosts the Alpha oil shale deposit (described).|||||Cross-bedded sandstone with minor conglomerate, siltstone, mudstone, coal and oil shale (torbanite).|
27129|Colinlea Sandstone|73163|5|Briefly described|p468|Lopingian|Lopingian|Springsure Shelf.||||Lateral equivalent of the Colinlea Sandstone equivalent.|Predominantly composed of quartz, lower part is feldspar-deficient, upper part contains more feldspar. Basal conglomerate contains chert, volcanic rocks, subordinate quartzite.|
27129|Colinlea Sandstone|73472|6|Mentioned|p115-116|Wuchiapingian|Capitanian|Galilee Basin.||||Overlain by Peawaddy Formation. Equivalent to Betts Creek beds, Catherine Sandstone, Ingelara Formation, Freitag Formation, and Aldebaran Sandstone.||
27129|Colinlea Sandstone|73625|6|Mentioned|p19|Permian|Permian|Western Bowen Basin. Contains low-diversity floras of glossopterid and cordaitalean gymnosperms.||||||
33161|Collaroy Volcanics|23042|4|Described|p37,41,2,,64,73,Fig2||Early Permian|Underlying unit Connors Volcanics.||||||
33161|Collaroy Volcanics|60445|5|Briefly described|p5|Early Permian|Early Permian|Of the Connors Volcanic Group. Comprise dark grey to dark greenish or purplish grey mainly fine-grained, aphyric to slightly flow-banded porphyritic basalt to andesite containing some amygdaloidal zones and breccia lenses.||||||16-MAY-06
33161|Collaroy Volcanics|60473|5|Briefly described|Map Legend|Early Permian|Early Permian|Basalt to andesite; breccia lenses, dacite rhyodacite, rhyolite. Dacitic ignimbrite or crystal-lithic tuff.||||||29-SEP-04
33161|Collaroy Volcanics|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Mostly basalt, including pillow lava and volcaniclastics; minor fossiliferous, impure limestone and calcareous sandstone and mudstone.||||||
33161|Collaroy Volcanics|60787|5|Briefly described|p9|Permian|Permian|||||||
33161|Collaroy Volcanics|61035|5|Briefly described|p8-11|Permian|Artinskian|Of the Lizzie Creek Volcanic Group. Age suggested by fossils in unit. Geological Province: Connors Sudprovince. Mafic volcanics with minor sandstone, volcanic breccia, + fossiliferous limestone.||||||07-FEB-11
33161|Collaroy Volcanics|65388|3|Fully described|p146-149; p31, 59, 81, 85, 90, 123, 135|Early Permian|Early Permian|Of Lizzie Creek Volcanic Group, Connors Arch. Extend from south of Pint Pot Mountain to north of Undercliff Station. Occupy a broad valley formed by Murray and Collaroy Creeks from which the name is derived. In faulted contact with Leura Volcanics. Unconformably overlie Mountain View Volcanics. Fossils suggest time equivalence to Artinskian Buffel Formation, Tiverton Formation. Correlations suggest this unit younger than Mount Benmore Volcanics. Mainly fine-grained, aphyric, locally amygdaloidal basalt or andesite flows and breccia. Probably shallow marine. See also p143, 232, 362, 447.||||||
33161|Collaroy Volcanics|68679|5|Briefly described|p353, p355, p360, p379|Permian|Permian|Forms a meridional belt ~50km long and up to 7km wide SE of Nebo, Connors Subprovince. Probably overlaps in age with lowermost Back Creek Group. Probably younger than Mount Benmore Volcanics and Carmila beds. Contains early Permian marine fossil bivalve fauna.||Lizzie Creek Volcanic Group.||Time-equivalent of Buffel and Tiverton Formations (interfingers with the latter). Is faulted against the Leura Volcanics.|Mainly aphyric, locally amygdaloidal basalt or andesite flows and breccia with possible pillows and monomict breccia that may be quench fragmented; locally interbedded with fossiliferous, sandy limestone and coquinite and massive labile sandstone.|
30003|Collingwood Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|282-246 Ma.|Unit in Collingwood Group.||||
30003|Collingwood Granite|23423|6|Mentioned|p281|||||||||
30003|Collingwood Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30003|Collingwood Granite|43070|5|Briefly described|p51|||of Cooktown Supersuite||||||
30003|Collingwood Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite.  Seriate to slightly porphyritic, cordierite(altered)-biotite granite.||||||
30003|Collingwood Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Collingwood Suite (Cooktown Supersuite). Age: 282-264Ma (Rb-Sr). Med. to coarse-grained, seriate to moderately porphyritic cordierite (altered)-biotite granite; tourmaline commonly very abundant at contact; S-type. More lithology included.||||||07-FEB-11
30003|Collingwood Granite|69592|6|Mentioned|p249 Fig.4.34|Permian|Permian|Time-space diagram of Kennedy Igneous Association granitoids relative to Permian deformation in the Palmer-Barron Subprovince.||||||
30003|Collingwood Granite|69593|5|Briefly described|p479, p482, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Dating by Murgulov (2006). Sm-Nd isotope data tabulated.|275.9 +/- 4 Ma (LA-ICP-MS U-Pb zircon).|Collingwood Suite.|||S-type granitoids.|
30003|Collingwood Granite|72983|4|Described|p3, p7, p28-33|Capitanian|Wordian|Kennedy Igneous Association. Hodgkinson Province, eastern. Cape York region. Murgulov (2006) reported a U-Pb LAM-MC-ICP-MS zircon age of 275.9 +/- 4 Ma for a sample close to Collingwood mine, which is similar in age to the Charlotte Granite. Several other superseded dates include K-Ar and Rb-Sr ages. Hosts significant tin mineralisation.|262.8 +/- 1.4 Ma SHRIMP U-Pb|Cooktown Supersuite|||Includes medium-grained, porphyritic, leucocratic muscovite-biotite granite.|
36724|Collingwood Suite|23423|5|Briefly described|Table 7.1 p240|||Of Collingwood Group.||||||
36724|Collingwood Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Early Permian|Of the Cooktown Supersuite. Contains the Collingwood Granite. Age: 282-264Ma (Rb-Sr). Lithological details presented. S-type.||||||07-FEB-11
36724|Collingwood Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Collingwood Granite.||S-type granitoids.|
27980|Collins Creek Rhyolite|22675|4|Described|p54|Late Carboniferous|Late Carboniferous|Bulgonunna Volcanic Group||||||
27980|Collins Creek Rhyolite|23504|5|Briefly described|Map Legend||Carboniferous|of Bulgonunna Volcanic Group.||||||
27980|Collins Creek Rhyolite|43391|5|Briefly described|Map legend||Late Carboniferous|Of the Bulgonunna Volcanic Group. Rhyolitic ignimbrite.  Geological Province: Coastal Ranges Igneous Province.||||||23-JUN-04
27980|Collins Creek Rhyolite|43706|5|Briefly described|p6||Late Carboniferous|||||||
27980|Collins Creek Rhyolite|43727|5|Briefly described|Table 14,p50|||||||||
27980|Collins Creek Rhyolite|43936|5|Briefly described|Map Legend||Carboniferous|Of Bulgonunna Volcanic Group||||||
27980|Collins Creek Rhyolite|60659|5|Briefly described|p16|||Of the Bulgonunna Volcanic Group. Crystal-rich to very crystal-rich and lithic clast-free to lithic-poor, moderately massive welded rhyolitic ignimbrite. Part of the Locharwood association. Of the Bulgonunna Province.||||||07-FEB-11
27980|Collins Creek Rhyolite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
27980|Collins Creek Rhyolite|70740|5|Briefly described|p82 fig 50, p85-p88, p105-p106, p122|||Distinguished from the Hidden Valley Rhyolite by its more crystal rich and biotite abundance.||Bulgonunna Volcanic Group||Overlies the Stones Creek Volcanics. Overlain by the Hidden Valley Rhyolite.|Dark to very dark bluish-grey, crystal-rich to very crystal-rich and lithic poor, moderately massive, thoroughly welded rhyolitic ignimbrite that is characterised by abundant and conspicuous embayed quartz.|
36178|Collins Weir Rhyolite|23506|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
36178|Collins Weir Rhyolite|72983|4|Described|p1, p7, p14, p16-21|Kungurian|Artinskian|Kennedy Igneous Association. Cairns region. Intrusive complex comprising numerous northwesterly trending dykes and irregular, thicker, elongate microgranite intrusions. Previously labelled the 'Parada Dyke Swarm' by Best, 1962). Is the youngest Paleozoic unit in the local area; part of the youngest group in the Cairns hinterland. Suspected coeval with Tinaroo Granite, Hope Vale Granite, Featherbed Volcanic Group and Nychum Volcanics.|281.9 +/- 1.2 Ma SHRIMP U-Pb|||Intrudes Atlanta Granite and Parada Granite. Some felsic dykes cut the Walsh Bluff Volcanics.|Porphyritic rhyolite and microgranite.|
27130|Collopy Formation|23422|5|Briefly described|p180, p205 Table 6.3|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|23430|5|Briefly described|p506|||Burdekin Basin Province.||||||
27130|Collopy Formation|23504|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|23893|5|Briefly described|p9 Fig. 4|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Late Devonian|Geological Province: Burdekin Basin.||||||
27130|Collopy Formation|24613|2|Defined|p6 Fig. 3, p9 Fig. 4, p89|Early Carboniferous|Late Devonian|Unconformably overlies granitoids of Ravenswood Granodiorite Complex. Max.thickness: 1000m. Geological province: Burdekin Basin. Poorly sorted, micaceous sublabile, lithic and lithofeldspathic pebbly sandstone - detailed lithology included. See also p135||||||07-FEB-11
27130|Collopy Formation|30148|6|Mentioned|p36|||Triassic age||||||
27130|Collopy Formation|32553|4|Described|p40|||||||||
27130|Collopy Formation|36472|6|Mentioned|Map legend|Triassic|Triassic|||||||
27130|Collopy Formation|39686|6|Mentioned|p73|||||||||
27130|Collopy Formation|39735|6|Mentioned|p19|||||||||
27130|Collopy Formation|41774|6|Mentioned|p32|||||||||
27130|Collopy Formation|42245|6|Mentioned|p35|||||||||
27130|Collopy Formation|42295|5|Briefly described|Fig.2 P5|||||||||
27130|Collopy Formation|43093|6|Mentioned|Appendix 1|||Mentioned in terms of relationship to Drynoch Granite||||||
27130|Collopy Formation|43935|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|43936|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27130|Collopy Formation|44061|4|Described|Table 6||Mesozoic|||||||
27130|Collopy Formation|45151|5|Briefly described|Table 10|||See also P15.||||||
27130|Collopy Formation|48904|2|Defined|p61|Mesozoic|Mesozoic|Prob. Mesozoic||||||
27130|Collopy Formation|63154|5|Briefly described|p285 Fig. 5|Devonian|Devonian|Geological province: Charters Towers Province. Mixed shallow marine sediments.||||||
27130|Collopy Formation|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Burdekin Basin.||||||
27130|Collopy Formation|68576|5|Briefly described|Q_11: p43|Late Devonian|Middle Devonian|Mingela area. An outlier of the Burdekin Basin.|||||Fluviatile, quartzose sandstone.|
27130|Collopy Formation|68731|5|Briefly described|184 Fig 3.98, p185 Tb 3.4, p187|Upper Devonian|Middle Devonian|> 200 m thick. Alluvial fan to upper, sand dominated, alluvial plain. Contains rare siltstone lenses with plant fragments. Has not been assigned to a Group.||||Nonconformable on the Ravenswood Granodiorite. Equivalent to the Fanning River Group.|Comprises coarse to very coarse micaceous, feldspathic to lithic sandstone, variably pebbly with local pebble lags. Pebble to boulder conglomerate in lower interval.|03-JUL-14
78919|Colodon Granodiorite|65388|3|Fully described|p307-308, p237, 238, 295, 301, 303, 304|Early Triassic|Late Permian|Of Wingfield Suite, Rawbelle Batholith area. Previously included in the Wingfield Adamellite. Intrudes Mount Bulgi Conglomerate Member of Camboon Volcanics. In contact with Wingfield Granite, Kooyong Gabbro and Glencoe Gabbro. Encloses the Tecoma Granodiorite and Hefferon Creek Gabbro. Contact relationships all masked by soil cover. Age assumed. Two 'Colodon Granodiorite samples' plot with Tecoma Granodiorite and Coonambula Suite rocks, suggesting distribution of these units needs review. Outcrop poor. Ranges from quartz monzodiorite to granodiorite. Distinguished on radiometric response. See also p320, 332, 333, 338, 339-340.||||||
78919|Colodon Granodiorite|68679|5|Briefly described|p410, p416-420|||Southern part of the northern New England Orogen. Far north of the Rawbelle Batholith. Locally exhibits primary igneous foliation. Two samples plot within Coonambula Suite. Geochemistry plot.||Wingfield Suite.||Encloses Tecoma Granodiorite (?older rafts) and Hefferon Creek Gabbro (probably intruded by it). May be intruded by Kildare Granodiorite.|Hornblende-biotite to biotite granodiorite to quartz monzodiorite; minor gabbro. Strongly foliated on western margin (probably igneous).|
74685|Colosseum Quartz Monzodiorite|64556|6|Mentioned|p56|Late Triassic|Late Triassic|Age: 225.0+/-1.8Ma. On MIRIAM VALE 1:100K sheet.||||||07-FEB-11
74685|Colosseum Quartz Monzodiorite|65452|5|Briefly described|p6 Fig.2, p7 Tb.2, p29|Late Triassic|Late Triassic|Geochemistry briefly described.|225 +/- 1.8 Ma (Black, unpublished).||||Fine- to medium-grained, hornblende quartz monzodiorite.|
74685|Colosseum Quartz Monzodiorite|67203|5|Briefly described|p4|Triassic|Triassic||225 +/- 1.8 Ma (Black, unpublished).||||Fine- to medium-grained, hornblende quartz monzodiorite.|
74685|Colosseum Quartz Monzodiorite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||225.0 +/- 1.8 Ma U-Pb SHRIMP||||Pale pinkish grey to pale grey, fine to medium grained, uneven-grained to slightly porphyritic biotite-hornblende granodiorite to quartz monzogranite; locally granophyric; commonly partly altered; locally fine-grained dioritic enclaves.|05-SEP-14
74685|Colosseum Quartz Monzodiorite|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Mentioned as being similar to the Walily Creek Quartz Monzodiorite, thereby justifying the latter unit's age attribution to the Late Triassic.|225.8 +/- 1.8 Ma (SHRIMP U-Pb: Black, unpub).||||Mostly pale pinkish-grey to pale grey, fine- to medium-grained, equigranular to slightly porphyritic biotite and hornblende granodiorite to monzodiorite, with some tonalite and granite; may contain abundant mafic inclusions; locally granophyric.|
23497|Columbia Creek Complex|22847|3|Fully described|p 45|||||||||
23497|Columbia Creek Complex|23422|5|Briefly described|p173, p210 Table 6.6|Ordovician|Ordovician|Of Columbia Creek Supersuite.||||||
23497|Columbia Creek Complex|23430|5|Briefly described|Table 14.2 p460.||Ordovician|Zircon crystallisation 464+/-5 Ma. Ravenswood Batholith Province||||||
23497|Columbia Creek Complex|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 455. S-Type.||||||
23497|Columbia Creek Complex|42633|5|Briefly described|Table 1 P9|||Reserved.||||||
23497|Columbia Creek Complex|42750|2|Defined|p37||Middle Ordovician|||||||
23497|Columbia Creek Complex|43093|4|Described|Appendix 1|||Pb-U age of 464+/-5Ma||||||
23497|Columbia Creek Complex|43259|4|Described|Appendix 1,p48.||Ordovician|U-Pb zircon age is 464+/-5 Ma. Middle Ordovician.||||||
23497|Columbia Creek Complex|43934|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
23497|Columbia Creek Complex|62521|5|Briefly described|p16, p48, p52-53|Middle Ordovician|Middle Ordovician|Age: 464+/-5Ma (U-Pb). Geological Province: Ravenswood Batholith. Contains granites of the 'peraluminous' type; ranging from muscovite-bearing pegmatites to two-mica granodiorite; migmatitic xenoliths. See also p7 Tb. 1.||||||14-JAN-08
23497|Columbia Creek Complex|68576|6|Mentioned|Q_11: p42|||Charters Towers.||||||
23497|Columbia Creek Complex|68731|5|Briefly described|p144 Fig 3.43, p147|Middle Ordovician|Middle Ordovician|Crops out in the Ravenswood Batholith north of Charters Towers. Contains inherited zircon populations at ~ 600 Ma and 1840 Ma. Has similar geochemistry and setting to the Two Creek Granodiorite.|464 +/- 5 Ma, SHRIMP crystallisation age||||Comprises upper amphibolite grade gneiss, migmatite and granite.|
23497|Columbia Creek Complex|69952|5|Briefly described|p94-95, p98, p103|||Charters Towers.|464 +/- 5 Ma (Hutton et al., 1994).|||Intrudes Charters Towers Metamorphics.|Includes granite (dykes).|
38174|Columbia Creek Supersuite|23422|4|Described|p173, p210 Table 6.6|Middle Ordovician|Middle Ordovician|Includes Charters Towers and Argentine Metamorphics.||||||
38174|Columbia Creek Supersuite|68553|6|Mentioned|Map legend|Early Silurian|Ordovician|Charters Towers Province. This unit (in part), as well as the Chipley, Brittany, Hogsflesh and Lavery Creek Supersuites; Schreibers and Sunburst Suites; the Lynwater Complex; and various Ordovician ungrouped plutonic units, are all mapped under the same symbol, Ogm. It is also (in part) mapped with Mingela Granodiorite and various Early Silurian ungrouped plutonic units under the symbol OSgm.||||||
38174|Columbia Creek Supersuite|68900|6|Mentioned|p4|Early Silurian|Ordovician|Drummond Basin.||||||
38174|Columbia Creek Supersuite|70749|5|Briefly described|p48|||SHRIMP U-Pb zircon maximum depositional age.|~464 Ma (Hutton and Crouch, 1993).|||Adjacent to (?intrudes) Charters Towers Metamorphics.||
28465|Comet Volcanics|41689|6|Mentioned|Table 1|||||||||
28465|Comet Volcanics|42054|6|Mentioned|p272|||||||||
82211|Condamine Alluvium|72921|6|Mentioned|p24.|||Interpreted as a shallow ?Pleistocene aquifer.||||||
82211|Condamine Alluvium|73113|5|Briefly described|p. 3, 7, 19, 21, 26-29, 35, 38-41...|||Incised into the Walloon Coal Measures by up to 120 m. Basal contact zone forms the ""Condamine Alluvium transition zone"" ca 1-15 m thick. Heavily utilised for groundwater supply. More locations: p. 43-45, 48, 51-52, 62, 85-86, 88-89, 98, 114, 118-122, 128-129, 137-138, 143, 145-148, 151-152, 158, 160-161, 166, 171-172, 197, 201||||Unconformably underlain by Walloon Coal Measures.|Includes basal alluvial clays.|
82211|Condamine Alluvium|73200|4|Described|p531-535, p538, p540, p542 Fig.14, p543|Quaternary|Quaternary|Divided into two subunits: poorly sorted sheetwash alluvial deposits, and overlying water-bearing granular floodplain alluvium. Radiocarbon dating of 44 +/- 2 to 45 +/- 2 Ka from a primary tributary of the Condamine River constrains deposition to during or shortly after the Late Pleistocene (Price and Sobbe, 2005). Basal clay-rich horizon referred to as the Transition Zone where contact with the Walloon Coal Measures is unclear, divided into three zones of bleached and oxidised clays with silt, clayey sand, lesser cemented sand and layers of pebbles to cobbles interpreted as weathered Jurassic sediments and Cenozoic clay deposits. Condamine Alluvium depicted as 130m thick and the Transition Zone being 0-30m thick (p532 Fig.2). LA-ICP-MS detrital zircon U-Pb ages of 162.0 +/- 7.5 Ma, 149.9 +/- 5.5 Ma and 154.9 +/- 8.9 Ma from the Transition Zone.|44 +/- 2 Ka - 45 +/- 2 Ka radiocarbon dating|||Angularly overlies the Walloon Coal Measures, Kumbarilla Beds.|Comprises fine-grained, poorly sorted sheetwash alluvial deposits and overlying granular floodplain alluvium. Includes a basal clay-dominated horizon, overlain by coarse sand in a fining upwards sequence.|
79454|Condamine Sandstone|70628|6|Mentioned|p952,964|Jurassic|Jurassic|Said to be informally named [by Sliwa et al., 2014]. Unclear if Condamine Sandstone is in Taroom Coal Measures or Juandah Coal Measures. Neither ubiquitous nor contemporaneous across the eastern Surat Basin and thus should not be recognised within a formal sequence stratigraphic framework. Intra-Walloon Subgroup coarse-grained unit.|||||Coarse-grained sandstone.
|29-JUN-16
81115|Condor Oil Shale|69599|5|Briefly described|p588 Fig.8.7(b), p590|Cenozoic|Cenozoic|Green and Bateman (1981); Green et al. (1984). Northern Hillsborough Basin. [Consistently capitalised, implying the authors regard it as a formal unit.] Comprises seven informal units, none of which is ranked as Member. Stratigraphic columns.||||||19-JUN-19
25854|Cone Creek Metabasalt Member|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Marraba Volcanics (Malbon Group). Metabasalt, quartzite.||||||
25854|Cone Creek Metabasalt Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25854|Cone Creek Metabasalt Member|30530|2|Defined|p515|Proterozoic|Proterozoic|||||||
25854|Cone Creek Metabasalt Member|35295|6|Mentioned|Fig.2|||||||||
25854|Cone Creek Metabasalt Member|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25854|Cone Creek Metabasalt Member|38350|6|Mentioned|p10|||||||||
25854|Cone Creek Metabasalt Member|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25854|Cone Creek Metabasalt Member|39496|5|Briefly described|p5|||||||||
25854|Cone Creek Metabasalt Member|39622|6|Mentioned|Appendix|||||||||
25854|Cone Creek Metabasalt Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25854|Cone Creek Metabasalt Member|45161|6|Mentioned|p40|||||||||
25854|Cone Creek Metabasalt Member|45166|5|Briefly described|p20|||||||||
25854|Cone Creek Metabasalt Member|49041|6|Mentioned|Table 4|||||||||
25854|Cone Creek Metabasalt Member|50100|5|Briefly described|p17|Statherian|Statherian|Of the Marraba Volcanics.  Geological Province: Eastern Fold Belt.||||||20-JAN-05
25854|Cone Creek Metabasalt Member|63866|6|Mentioned|p62, p65|||Mitakoodi Anticline. Also referred to as the Cone Creek Basalt on p62.||Marraba Volcanics||||
25854|Cone Creek Metabasalt Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin||Malbon Group.|||Metabasalt.|
25854|Cone Creek Metabasalt Member|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Is overlain by Mount Start Member.|Metabasalt. Basalt breccia and pillow lava are mapped as a separate unit.|
25854|Cone Creek Metabasalt Member|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Is overlain by Mount Start Member.|Metabasalt. Basalt breccia and pillow lava are mapped as a separate unit.|
25854|Cone Creek Metabasalt Member|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Partially equivalent to Mount Start Member.|Metabasalt, basalt breccia and pillow lava.|30-JUL-20
25854|Cone Creek Metabasalt Member|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Partially equivalent to Mount Start Member.|Basalt breccia and pillow lava and metabasalt.|
25854|Cone Creek Metabasalt Member|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Marraba Volcanics||Underlies Timberoo Member.|Metabasalt.|
25854|Cone Creek Metabasalt Member|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Marraba Volcanics||Underlies Timberoo Member.|Metabasalt.|
70424|Conella Granodiorite|68421|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||Intrudes the Duckpond Road Metamorphics.|Porphyritic hornblende-biotite monzogranite; foliated in places.|
70424|Conella Granodiorite|68679|5|Briefly described|p409|||Wandilla Province. Possibly Carboniferous-Permian.|||||Locally foliated, porphyritic hornblende-biotite monzogranite to granodiorite.|
70424|Conella Granodiorite|73450|6|Mentioned|p22|||Interpreted to pre-date Borilla Granite.||||||
36261|Confluence Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36261|Confluence Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 282. I-Type.||||||
36261|Confluence Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36261|Confluence Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Medium- to coarse-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
27642|Conical Knob Microgranite|23032|4|Described|p44||Early Carboniferous|||||||
27642|Conical Knob Microgranite|23291|4|Described|p50, p98 Tb 3.11|Carboniferous|Early Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
27642|Conical Knob Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 41. I-Type.||||||
27642|Conical Knob Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27642|Conical Knob Microgranite|40542|6|Mentioned|p97|||||||||
27642|Conical Knob Microgranite|43259|4|Described|Appendix 1,p18.||Carboniferous|||||||
27642|Conical Knob Microgranite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
27642|Conical Knob Microgranite|43740|4|Described|p27||Carboniferous|||||||
27642|Conical Knob Microgranite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27642|Conical Knob Microgranite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Overlain by Old Man Rhyolite. Overlies Mount Rous Microgranodiorite.||||||14-MAY-04
27642|Conical Knob Microgranite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province. In East-West Ring Dyke of the Bagstowe Ring Structure.|||||Pink, porphyritic hornblende-biotite microgranite.|
27642|Conical Knob Microgranite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Pink, porphyritic, hornblende-biotite microgranite.|
27642|Conical Knob Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Hornblende-biotite microgranite. I-type.|
23501|Connie May Dolerite|23291|4|Described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Western Georgetown Region. Age: ca.280Ma. Geological Province: Georgetown Region.||||||18-JUN-15
23501|Connie May Dolerite|23430|5|Briefly described|p518|||||||||
23501|Connie May Dolerite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
23501|Connie May Dolerite|40542|6|Mentioned|p97|||||||||
23501|Connie May Dolerite|43740|4|Described|p31||Carboniferous|||||||
23501|Connie May Dolerite|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Olive green porphyritic augite dolerite.|
70433|Connors Volcanic Group|60445|5|Briefly described|p5|||Supersedes Connors Volcanics. Includes Mountain View Volcanics (base), Whelan Creek, Leura and Collaroy Volcanics. Consists of rhyolitic crystal-lithic tuff, rhyodacitic tuff, conglomerate and andesitic breccia. Overlain by Lizzie Creek Volcanic Group.||||||20-MAR-13
70433|Connors Volcanic Group|61035|5|Briefly described|p3 Fig. 1, p6|Carboniferous|Carboniferous|Includes; Lotus Creek Rhyolite, Clive Creek Volcanics, Mountain Creek Volcanics, Broadsound Range Volcanics, Mount Whelan Volcanics, Leura Volcanics. Geol Prov: Connors Sudprovince.||||||07-FEB-11
70433|Connors Volcanic Group|65388|5|Briefly described|p85, 86, 90 Fig.35, 83 Fig.33, 110, 362|||Connors Arch. To be used for all of the largely intermediate to felsic Carboniferous volcanic succession, from Cycle 1 through to Cycle 3A of Dear (1994a). Includes Clive Creek Volcanics, Mountain View Volcanics, Broadsound Range Volcanics, Whelan Creek Volcanics, Lotus Creek Rhyolite, Leura Volcanics and Tartrus Rhyolite and  possibly Macksford Volcanics.||||||
70433|Connors Volcanic Group|65706|4|Described|p13 Tb.1, p17 Tbl.1,|Early Carboniferous|Late Devonian|||||Is intruded by Urannah Igneous Complex; unconformably underlies Lizzie Creek Volcanic Group.|Felsic to mafic volcanic rocks; rhyolitic to andesitic flows, high level intrusives and volcaniclastic rocks including ignimbrite, volcanic breccia.|
70433|Connors Volcanic Group|68359|6|Mentioned|p9|||||||||
70433|Connors Volcanic Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Carboniferous|Connors Subprovince.||||Is intruded by Withersfield Quartz Syenite.||
70433|Connors Volcanic Group|68679|5|Briefly described|p347,p351,p353,p355,p360-361,p375,p379|Permian|Carboniferous|Withnall et al. (2009); previously the Connors Volcanics of Malone et al. (1964) and others. Incorporates most of the Carboniferous to earliest Permian volcanics in the northern part of the Connors Subprovince, northern New England Orogen. An age determination by Cross et al., (2012) for "Connors Volcanic Group(?)" is 289.5 +7/-6 Ma from 10 heterogeneous zircons.|c.295 Ma.||Macksford Andesite[=Volcanics]; Lotus Creek, Tartrus Rhyolites; Leura, Broadsound Range, Mountain View, Mount Whelan[=Whelan Creek], Clive Creek Volcanics.|Is intruded by the Dacey Granite and Burwood Complex.||
70433|Connors Volcanic Group|68901|5|Briefly described|p64-67, p145, p2, p4|Permian|Carboniferous|northern New England Orogen, Bowen Region. Dacite sample dated to try to determine whether it was from this unit or Lizzie Creek Volcanic Group, but only 12 grains analysed and results are inconclusive. SHRIMP results and analysis discussed in detail.|~289 Ma reconnaissance age||||Dark-grey, very fine-grained, slightly porphyritic dacite, containing smal;l white feldspar phenocrysts and scarce lithic fragments.|04-OCT-18
70433|Connors Volcanic Group|69952|6|Mentioned|p85|Permian|Carboniferous|New England Orogen.||||||
70433|Connors Volcanic Group|70673|4|Described|p6, p8-10, p130-133|Permian|Late Carboniferous|Withnall et al. (2009). Previously Connors Volcanics. Bowen Region/Connors Subprovince. Forms rocky, hilly country.|306.5 +/- 1.6 Ma (SHRIMP U-Pb zircon).|||Adjacent to Lizzie Creek Volcanic Group.|Includes locally flow-banded, autobrecciated and intensely jointed rhyolite, interlayered with dark grey, very fine-grained, slightly porphyritic dacite.|
70433|Connors Volcanic Group|71264|6|Mentioned|p581 Fig.4|Carboniferous|Carboniferous|Bowen Basin.||||||
70433|Connors Volcanic Group|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|289 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite, rhyolite.|
70433|Connors Volcanic Group|73036|5|Briefly described|Map legend|Early Permian|Carboniferous||||||Felsic to mafic volcanic rocks; rhyolitic to andesitic flows, high-level intrusives, and volcaniclastic rocks including ignimbrite.|
70433|Connors Volcanic Group|73037|5|Briefly described|Map legend|Early Permian|Carboniferous||||||Felsic to mafic volcanic rocks; rhyolitic to andesitic flows, high-level intrusives, and volcaniclastic rocks including ignimbrite.|
70433|Connors Volcanic Group|73197|5|Briefly described|p465 Fig.4, p467|Carboniferous|Carboniferous|New England Orogen, northern. Connors Subprovince. Unit belongs to the Currabubula-Connors Arc. Equivalent to the Torsdale Volcanics in the Auburn Subprovince.|||||Predominantly rhyolitic to dacitic ignimbrites with minor lava flows, rare andesitic and basaltic lavas and volcaniclastic rocks.|
24864|Constance Sandstone|22673|6|Mentioned|66|||||||||
24864|Constance Sandstone|22680|6|Mentioned|84,86,87|||Geol province: Mount Isa Basin. Of the McNamara Group.||||||07-AUG-06
24864|Constance Sandstone|23065|6|Mentioned|4, 17|||||||||
24864|Constance Sandstone|23393|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Group.  Referred to as Constance Range Sandstone in Fig. 7, p28.||||||
24864|Constance Sandstone|23405|5|Briefly described|p586, 587|Statherian|Statherian|Of South Nicholson Group. 1591+/-10Ma from tuffaceous conglomeratic unit near base.||||||11-NOV-10
24864|Constance Sandstone|23937|5|Briefly described|p76 App. 1|||Of the South Nicholson Group.  Overlain by Mullera Formation.  See also p83 Appendix 1.||||||
24864|Constance Sandstone|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Flemington Subgroup? (South Nicholson Group).  Contains 5 sandstone/siltstone members.||||||
24864|Constance Sandstone|26310|4|Described|p3, 10, Table 1|Proterozoic|Proterozoic|Conformably underlies the Mullera Formation; underlies: Gold Creek Volcanics.  Overlies Lawn Hill Formation.  Maximum Thickness: 5,500 feet. Sandstone, greywacke.||||||09-AUG-04
24864|Constance Sandstone|30479|6|Mentioned|Fig.17|||Precambrian age.||||||07-AUG-06
24864|Constance Sandstone|32660|5|Briefly described|Table 5|||||||||
24864|Constance Sandstone|33387|6|Mentioned|p349|||||||||
24864|Constance Sandstone|35640|6|Mentioned|Map legend|Adelaidean|Adelaidean|Carpentarian?||||||
24864|Constance Sandstone|36003|6|Mentioned|Fig.8|||||||||
24864|Constance Sandstone|36012|3|Fully described|Table 4|||See also p16.||||||07-AUG-06
24864|Constance Sandstone|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
24864|Constance Sandstone|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
24864|Constance Sandstone|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24864|Constance Sandstone|38348|6|Mentioned|p24|||||||||
24864|Constance Sandstone|38584|4|Described|p19|||See also p18.||||||17-JUL-06
24864|Constance Sandstone|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the South Nicholson Group.  Fine to medium quartz sandstone, some coarse-grained; conglomerate beds; lenses of pebble to boulder conglomerate. Unconformably overlies Lawn Hill Fm. and its Widdallion Sandstone Member; conformably overlain by Mullera Fm.||||||10-JAN-05
24864|Constance Sandstone|39445|5|Briefly described|p56|||See Table 3||||||
24864|Constance Sandstone|39497|4|Described|p15|||See also p11.||||||07-AUG-06
24864|Constance Sandstone|39685|6|Mentioned|Fig.1|||||||||
24864|Constance Sandstone|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24864|Constance Sandstone|39925|6|Mentioned|p329|||See also Fig.2.||||||
24864|Constance Sandstone|40623|5|Briefly described|p112|||||||||
24864|Constance Sandstone|41721|3|Fully described|p29|||Of South Nicholson Gp. Contains the Pandanus, Wallis and Bowthorn Siltstone Members. Unconformably overlies Fickling Gp; disconformably overlies Doomadgee Fm. Thickness: >1000m. Geol.prov:  South Nicholson Basin. Mainly med.-grained quartz sst/lithic sst||||||02-AUG-07
24864|Constance Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
24864|Constance Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of South Nicholson Group. Of "Mid Proterozoic" age.||||||07-AUG-06
24864|Constance Sandstone|44210|14|Not recorded|Tb.1|||Equivalent to Pilpah Sandstone.||||||
24864|Constance Sandstone|44271|2|Defined|p39-41,55|||See also Lexicon. Overlies Wollogorang Formation. Unconformably overlain by Lawn Hill Formation.||||||
24864|Constance Sandstone|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
24864|Constance Sandstone|44274|2|Defined|Tb.2,p9,10,15,16,map|||||||||
24864|Constance Sandstone|44275|14|Not recorded|Map Legend|||||||||
24864|Constance Sandstone|44280|2|Defined|p5,6,7,Tb.1,map|||||||||
24864|Constance Sandstone|44281|14|Not recorded|Map Legend||Neoproterozoic|||||||
24864|Constance Sandstone|44290|14|Not recorded|p439|||||||||
24864|Constance Sandstone|44305|14|Not recorded|p.6,8,14-15|||(E53-8). opp.6,18.||||||
24864|Constance Sandstone|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
24864|Constance Sandstone|44482|14|Not recorded|p.5,6,8,opp.p.6, map|||(E53-12). See also p.9,13,16, for more details.||||||
24864|Constance Sandstone|44483|5|Briefly described|map legend|||Upper(?) Proterozoic.||||||
24864|Constance Sandstone|44751|14|Not recorded|p302|||||||||
24864|Constance Sandstone|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
24864|Constance Sandstone|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of South Nicholson Group.||||||
24864|Constance Sandstone|44989|2|Defined|p.116-121||Neoproterozoic|Tb.II. On many pages. Upper Proterozoic. Overlies Lawn Hill Formation unconformably; and o/lies Wollogorang Formation; underlies Mullera Formation.||||||07-AUG-06
24864|Constance Sandstone|45052|2|Defined|p71|Adelaidean|Adelaidean|||||||
24864|Constance Sandstone|45079|6|Mentioned|p9|||Precambrian age. Map legend on p9.||||||07-AUG-06
24864|Constance Sandstone|45166|5|Briefly described|p33|||||||||
24864|Constance Sandstone|45287|14|Not recorded|p.223,226-7,229|||||||||
24864|Constance Sandstone|46804|6|Mentioned|p154|||||||||
24864|Constance Sandstone|49001|6|Mentioned|p12|||||||||
24864|Constance Sandstone|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Accident Subgroup. White, yellow and brown, friable, medium, coarse and very coarse grained to granule sandstone; minor siltstone and shale.||||||
24864|Constance Sandstone|64443|6|Mentioned|p3|Calymmian|Calymmian|Probable lateral relationship with Mittiebah Sandstone.||Of the Accident Subgroup.||||14-MAY-14
24864|Constance Sandstone|65337|2|Defined|p9 Fig.5, p38 Table 5, pp50-51.|Mesoproterozoic|Mesoproterozoic|North-central MOUNT DRUMMOND area. Possible correlative of Mittiebah Sandstone. 75 - 1100 m thick.Two facies dominate most outcrops: coarse sandstones and lower-energy, deeper-water micaceous sandstone and siltstone. Remarkably similar to Roper Group.||Unit in Accident Subgroup.|Includes Pandanus and Wallis Siltstone Members; Hedleys, Burangoo and Schultz Sandstone Members.|Unconformably overlies Caulfield beds. Disconformably overlies Crow Formation. Is overlain by Mullera Formation.|Dominantly thickly-bedded, cross-bedded, medium- to coarse-grained, granule-rich and occasionally pebbly, quartz or sublithic sandstone; interbedded red to grey-green fine-grained sandstone to siltstone; minor shale.|
24864|Constance Sandstone|67323|5|Briefly described|p39, GIS attrib tbl, Solid Geology Map|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. South Nicholson Basin.|1589 +/- 10 Ma (maximum depositional age).|South Nicholson Group.|||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|67352|6|Mentioned|p12|Calymmian|Calymmian|Has an uncertain but probably lateral relationship with Mittiebah Sandstone.||Accident Subgroup||||
24864|Constance Sandstone|67539|5|Briefly described|p14, p15, p15 Fig.8|||Reduced in thickness by recognition of regional unconformity within the unit. The rocks below the unconformity are now excluded from Constance Sandstone, so now equivalent to the Schultz Sandstone Member of Rawlings & others (2008), which is thus rendered obsolete. Forms the base of the South Nicholson Group, south of the Elizabeth Creek Fault. Redefined to include the Bowthorn Siltstone Member which was declared obsolete by Rawlings and others (2008).||Of the South Nicholson Group.||Overlain by the Mullera Formation. Unconformably underlain by the Boodjamulla Formation, Wallis Siltstone and McNamara Group.||
24864|Constance Sandstone|68146|4|Described|p2, p6, p28, p34-41, p196-197, p211|||South Nicholson Region. Fig.150 on p106 (by I. Sweet, in preparation) places the Constance Sandstone at the top of the Wild Cow Subgroup, below an unconformity; Bowthorn Siltstone Member is included as a Member. Described as "lateral equivalent" to Schultz Sandstone Member; similar detrital zircon spectra. An earlier MDA of 1591 +/- 10 Ma (Page et al., 2000) comes from rocks now recognised as Burangoo Sandstone. Whole-rock Sm-Nd isotopic data tabulated.|1599 +/- 19 Ma; maximum depositional age.|Accident Subgroup.|Schultz Sandstone Member, Bowthorn Siltstone Member.|Unconformably overlies Wild Cow Subgroup.|Medium-grained, well-sorted quartz sandstone.|
24864|Constance Sandstone|68575|6|Mentioned|p18-19|||Previously included rocks now called the Burangoo Sandstone.||||Unconformably overlies Wild Cow Subgroup.||
24864|Constance Sandstone|69434|4|Described|p19:2-6, 8|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Widespread in QLD and NT. 75-1100m thick. Sandstone Members are distinguishable only by the intervening siltstone Members; where these latter are absent, the Formation is mapped as a single unit. Detrital zircon maximum depositional age.|<1591 +/- 10 Ma (Page et al., 2000).|Basal Accident Subgroup.|Schultz, Burangoo, Hedleys, Sandstone Members; Wallis, Pandanus, Siltstone Members.|Overlies Caulfield beds unconformably, and Crow Formation conformably to disconformably. Is overlain conformably by Mullera Formation.|Medium- to coarse-grained, granule-rich and occasionally pebbly, quartz or sublithic sandstone, interbedded with very fine-grained sandstone and siltstone. Sandstone intervals are typically thickly bedded and cross-bedded.|12-JUL-16
24864|Constance Sandstone|69591|4|Described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Previously included Hedleys Sandstone, Pandanus Formation, Burangoo Sandstone and Wallis Formation as Members. Fluvial to shelf deposits. Age by Page et al. (2000).|1591 +/- 10 Ma (maximum depositional age).|Wild Cow Subgroup.|Shultz Sandstone Member, Bowthorn Member.|Unconformably overlies Wallis Formation. Is overlain by Bowthorn Member or unconformably by Elizabeth Sandstone.|Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|69673|6|Mentioned|p56|||Maximum thickness of 1100m. Deposited in fluvial to shallow marine, tidal environment.||Accident Subgroup|||Quartz or sublithic sandstone, interbedded with sandstone and siltstone.|
24864|Constance Sandstone|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin. Five facies are mapped separately.||South Nicholson Group.||Unconformably overlies Doomadgee Formation (Fickling Group). Is overlain by Mullera Formation.|Sandstones, siltstone, shale, greywacke.|
24864|Constance Sandstone|70897|4|Described|p39-40, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|The basal member thins to the NW, due to onlap onto the Murphy Inlier, implying positive basement relief during deposition of early stages of the South Nicholson Group.|1591 +/- 10 Ma (maximum depositional age).|Basal South Nicholson Group.|Bowthorn, Wallis, Pandanus, Siltstone Members.|Overlies Lawn Hill Formation with an angular unconformity (locally disconformably).|Includes pebbly, coarse-grained, feldspathic sandstone.|
24864|Constance Sandstone|70968|5|Briefly described|p131 Fig.118, p132|Calymmian|Calymmian|May correlate with the Collara Subgroup.||Accident Subgroup.||||
24864|Constance Sandstone|71369|3|Fully described|p1, p4-9, p14-15, p19-20, p22-25, p27|Mesoproterozoic|Mesoproterozoic|See also p32-34, p36-37, p48-50. South Nicholson Basin. Mapped by Carter and Opik (1961); defined by them in Carter et al. (1961). The type section runs "from latitude 18deg 27'25"S, longitude 138deg17'00"E east-southeast about 4 miles to the base of the formation". Their type section coincides with the stratigraphic span of the Schultz Sandstone Member of Rawlings et al. (2008) who abandoned the Bowthorn Siltstone Member. This latter unit is resurrected and redefined as Bowthorn Member (Sweet, 2017). The Constance Sandstone now encompasses both Members. Two reference sections are detailed. Redefined in this study following recognition of an unconformity; the overlying part is now the Elizabeth Sandstone (Sweet, 2017). Note that Fig. 2e on p6 erroneously includes this unit in the Wild Cow Subgroup. Forms an escarpment in the Constance Range. Up to 970-1170m thick.||Accident Subgroup.|Bowthorn, Schultz Sandstone, Pandanus, Burangoo Sandstone, Hedleys Sandstone and Wallis Siltstone Members.|Unconformably overlies Wallis Formation. Is overlain unconformably by Elizabeth Sandstone (Accident Subgroup). Equivalent to the Mittiebah Sandstone.|Interbedded medium-grained sandstone and finer sandstone and mudstone.|20-FEB-18
24864|Constance Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1599+/-19 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24864|Constance Sandstone|72297|5|Briefly described|p749|||South Nicholson Basin. Poor source material; organic material has mostly reached an advanced stage of thermal maturity.|||||Includes shales.|
24864|Constance Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Schultz Sandstone Member.||Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Schultz Sandstone Member.|Overlain by Elizabeth Sandstone or Mullera Formation. Underlain by Wallis Formation.|Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Accident Subgroup.|Includes Schultz Sandstone Member.|Overlain by Elizabeth Sandstone or Mullera Formation. Underlain by Wallis Formation.|Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|Includes Schultz Sandstone Member.||Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72526|4|Described|p1-2, p7, p8, p33-55, p56, p85-87|Calymmian|Calymmian|U-Pb SHRIMP maximum depositional ages obtained from 3 samples. Age with smallest error recorded here. Other ages are within error of this one. Shown as located in the central and eastern parts of the South Nicholson Basin. ~75-1100 m thick and extends across the border between the NT and Qid. Possibly lateral correlative with Mittiebah Sandstone. Shown as part of the Accident Subgroup on p8 Fig.1.3. Previously included Wallis Siltstone Member, Burangoo Sandstone Member, Pandanus Siltstone Member and Hedleys Sandstone Member (Rawlings et al., 2008.|1591+/-18 Ma max. dep.age.|Accident Subgroup|Includes Bowthorn Member, Shultz Sandstone Member.|Unconformably overlies Wallis Formation, Wild Cow Subgroup, Caulfield beds, Fickling Group. Conformably overlain by Mullera Formation, NT. Unconformably overlain by Elizabeth Sandstone, Qld.|Includes green-grey claystone, siltstone and cross-bedded, medium to coarse-grained sandstone; fine to very coarse-grained sandstone, dominated by moderately sorted, subangular to subrounded, quartz and feldspar grains.|
24864|Constance Sandstone|72527|6|Mentioned|p7 Fig.1.4, p10, p20|Mesoproterozoic|Mesoproterozoic|Maximum depositional age from detrital zircons in the basal conglomerate. Source assumed to be tuffs in Lawn Hill Formation. Now mapped as No Mans Sandstone Member in the Mitchiebo region.|Max. dep. age: 1591+/-10 Ma.|Accident Subgroup|Hedley Sandstone Member, Pandanus Sandstone Member, Burangoo Sandstone Member, Wallis Sandstone Member, Schultz Sandstone Member.|Unconformably overlies Tobacco Member and Caulfield beds, underlies Mullera Formation and is unconformably laterally equivalent to Mittiebah Sandstone.|Includes sandstone.|
24864|Constance Sandstone|72912|4|Described|p5 Fig.3, p23-24, p27-34, p48.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin. Hydrocarbon sources from this unit remain unexplained. No information on date shown p33.|1590+/-10 Ma|Base of Accident Subgroup.||Partially, unconformably overlies Wallis Fm and is equivalent to Mittiebah Sandstone and underlying Mullera Formation.||
24864|Constance Sandstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p15, p17 Fig.9.|Mesoproterozoic|Mesoproterozoic|Part of the South Nicholson Basin. Mineral composition boxplots reveal dominant quartz, muscovite and microcline components. Shown as being in the central part of the Isa Superbasin. Identified in 5 wells in this study. See also p26.|1590 +/- 10 Ma|Accident Subgroup|Includes Bowthorn Member.|Unconformably overlies Wallis Formation. Underlies Mullera Formation and is laterally equivalent to Mittebah Sandstone.|Includes sandstone, dolomitic siltstone.|
24864|Constance Sandstone|72919|5|Briefly described|p1, p4-5, p47-52, p70, p94-95|Ectasian|Calymmian|South Nicholson Basin. The stratigraphic position and definition has been revised in several studies; included in the Accident Subgroup in NT and the Wild Cow Subgroup in QLD. New U-Pb SHRIMP zircon maximum depositional age (MDA) of 1468 +/- 36 Ma was reported herein from QLD, which represents the youngest MDA yet recorded for this unit. This is consistent with plausible bracketing ages of ca. 1266 Ma xenotime overgrowths and ca. 1483 Ma from a MDA in the underlying Crow Formation. Conversely, four previous MDAs were reported from QLD of 1599 +/- 19 Ma from Carson et al. (2011), and 1591 +/- 18 Ma, 1578 +/- 53 Ma, and 1569 +/- 37 Ma from Anderson et al. (2019). Two samples (unnamed sandstones) were collected and dated from an interval labelled undifferentiated South Nicholson Group in drillcore NTGS02/1; these were inferred to be probably of this unit (Constance Sandstone) or equivalent based on detrital zircon spectra (MDAs of 1605 +/- 18 Ma and 1610 +/- 35 Ma).|1468 +/- 36 Ma U-Pb SHRIMP|Accident Subgroup/Wild Cow Subgroup, South Nicholson Group|Schultz Sandstone Member, Wallis Sandstone Member, Burangoo Sandstone Member, Pandanus Sandstone Member, Hedleys Sandstone Member|Unconformably underlain by Wallis Formation and Crow Formation, including Tobacco Member (Wild Cow Subgroup). Overlain by Mullera Formation. Equivalent to Mittiebah Sandstone.||
24864|Constance Sandstone|72967|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group||||
24864|Constance Sandstone|73042|6|Mentioned|p2, p4, p9|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Accident Subgroup, South Nicholson Group|Bowthorn Member|Partly underlain by Wallis Formation unconformably. Conformably overlain by Mullera Formation.||
24864|Constance Sandstone|73043|6|Mentioned|p7 Fig.2|Mesoproterozoic|Mesoproterozoic|||South Nicholson Group||||
24864|Constance Sandstone|73083|6|Mentioned|p34-35|Mesoproterozoic|Mesoproterozoic|Has five members.||||Equivalent to Mittiebah Sandstone.||
24864|Constance Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Partial aquifer.||Accident Subgroup, South Nicholson Group|Schultz Sandstone Member, Bowthorn Member|Unconformably underlain by Wallis Formation (Wild Cow Subgroup). Unconformably overlain by Elizabeth Sandstone.||
36517|Continong microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 167.||||||
79366|Conway Volcanics|70740|4|Described|i, iii, p2, p8, p51, p74|Early Permian|Late Carboniferous|Drummond Basin. SHRIMP age derived from Black (1994) and is of  rocks now condisered to be near the base of this unit.  Name derived from the Conway Station. Outcrop characteristics discussed. Type section is nominated and described. Lithology and petrography discussed in detail. See also p82 fig 50, p83, p89-p93, p95, p115.|297.4 +/- 3.9 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Unconformably overlies the Bimurra Volcanics. Conformably overlain by the Whitestone Creek Dacite.|Crystal-rich, moderately to strongly welded dacitic to andesitic ignimbrites and moderately to coarsely porphyritic andesitic to dacitic lavas.|08-JAN-21
26489|Cooby Trachyte Member|23799|5|Briefly described|p9 Tb. 1, p56|Tertiary|Tertiary|Supersedes Cooby Trachyte.  Of the Main Range Volcanics.  Dark purplish-grey, very fine-grained trachyte.  Overlies Gomaren Basalt.  Geological Province: Main Range-Lamington Volcanic Province.||||||
26489|Cooby Trachyte Member|23800|5|Briefly described|Map Legend|Pliocene|Miocene|Of Main Range Volcanics.||||||
26489|Cooby Trachyte Member|24560|5|Briefly described|Map legend|Tertiary|Tertiary|Of the Main Range Volcanics.  Dark, purplish-grey, very fine-grained trachyte.||||||
26489|Cooby Trachyte Member|36579|6|Mentioned|Table 1|||||||||
26489|Cooby Trachyte Member|39969|6|Mentioned|p9|||||||||
26489|Cooby Trachyte Member|42525|5|Briefly described|Map legend|Miocene|Oligocene|Of the Main Range Volcanics.||||||15-JUL-04
26489|Cooby Trachyte Member|73450|4|Described|p4, p90-91, p95|Burdigalian|Rupelian|Northern Main Range. Forms deeply weathered, irregularly-shaped bodies in hilly terrain north of Toowoomba. Can be difficult to distinguish from the Gomaren Basalt. Interpreted as deposited in a steep-sided paleovalley and erupted from two vents. Whole-rock K-Ar age of 23.8 +/- 7 Ma (Webb et al., 1967).|23.8 +/- 7 Ma K-Ar|Main Range Volcanics|||Dark, fine-grained trachyte with rare plagioclase phenocrysts in a groundmass of sanidine, pyroxene, oqaque phases and chlorite, and is locally amygdaloidal or highly vesicular.|
24222|Coocerina Formation|39492|2|Defined|p30|Proterozoic|Proterozoic|||||||
24222|Coocerina Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
24222|Coocerina Formation|39997|6|Mentioned|p165|||||||||
24222|Coocerina Formation|40840|6|Mentioned|Map legend|||||||||
24222|Coocerina Formation|45166|4|Described|p32|||||||||
24222|Coocerina Formation|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Wonga Subprovince (Eastern Fold Belt Province).||||||
24222|Coocerina Formation|50332|5|Briefly described|p16, p20|Proterozoic|Proterozoic|Underlain by Dugald River Shale, overlain by Lady Clayre Dolomite. Consists of  calcareous black shale and scapolitic metasiltstone.||||||07-FEB-11
24222|Coocerina Formation|64250|5|Briefly described|p11, p13 fig 5, p18|||Mary Kathleen Belt (east).||Mount Albert Group||Overlies Knapdale Quartzite conformably. Underlies Lady Clayre Dolomite.|Calcareous black shale and scapolitic metasiltstone.|15-MAR-18
24222|Coocerina Formation|65387|6|Mentioned|p35|||||Unit in Mount Albert Group.||Overlies Knapdale Quartzite. Is overlain by Lady Clayre Dolostone.||
24222|Coocerina Formation|65396|5|Briefly described|p7, p17, p82, p84, p175, p183-184, p241|Calymmian|Statherian|Mary Kathleen Fold Belt.||Mount Albert Group||Conformably overlies Knapdale Quartzite. Is overlain by Lady Clayre Dolomite.|Calcareous black shale and scapolitic metasiltstone.|
24222|Coocerina Formation|67323|5|Briefly described|p15, p17-18; GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Mary Kathleen, Canobie Domains, Isa Superbasin. Appears as Cooncenra Formation [!?] in the Mount Isa Block Time-Space Plot.||Mount Albert Group.||Overlies Corella Formation. Time-equivalent to the Mount Roseby Schist.|Black shale, scapolitic siltstone, minor limestone.|
24222|Coocerina Formation|69056|5|Briefly described|p10, p55, Time-Space plot sheet|Statherian|Statherian|Mary Kathleen Domain.||Upper Mount Albert Group.||Overlies Knapdale Quartzite. Is overlain by Lady Clayre Formation. Time-equivalent of Mount Roseby Schist.||
24222|Coocerina Formation|69591|5|Briefly described|p43 Fig.2.31, p45, p46 Fig.2.39, p56|||Mary Kathleen Domain, Mount Isa Province. Part of Gun Supersequence. Deep marine deposits.||Mount Albert Group.||Overlies Knapdale Quartzite.|Black shale, laminated dolomitic siltstone with scapolite porphyroblasts, minor limestone.|
24222|Coocerina Formation|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Black shale, scapolitic siltstone and minor limestone.|
24222|Coocerina Formation|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Black shale, scapolitic siltstone and minor limestone.|
24222|Coocerina Formation|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Is overlain by Lady Clayre Formation.|Black shale, scapolitic siltstone and minor limestone.|
24222|Coocerina Formation|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group|||Black shale, scapolitic siltstone and minor limestone.|
24222|Coocerina Formation|73525|6|Mentioned|p4-5 Fig.2|||Mary Kathleen Domain.|||||Carbonates.|
24222|Coocerina Formation|73529|6|Mentioned|p5|||Calvert Superbasin, late. Deep marine setting.||Mount Albert Group||||
24222|Coocerina Formation|73553|6|Mentioned|p8 Fig.1.2.3|||Misspelt Coccerina Formation p187.||Mount Albert Group||||
23504|Cook Microgranite|23291|5|Briefly described|p98 Tb. 3.11|Late Carboniferous|Carboniferous|Part of the Bagstowe-Lochaber centred igneous structure (Glenmore Batholith area). Geological Province: Georgetown Region.||||||08-JUL-15
23504|Cook Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23504|Cook Microgranite|40542|6|Mentioned|p97|||||||||
23504|Cook Microgranite|43740|4|Described|p27||Carboniferous|||||||
23504|Cook Microgranite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Overlain by Mount Rous Microgranodiorite.||||||14-MAY-04
23504|Cook Microgranite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Bagstowe Ring Structure, Kennedy Province.|||||Pink to brown, abundantly porphyritic microgranite, locally containing sparse chlorite.|
23504|Cook Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Hornblende-biotite microgranite. I-type.|
27041|Cooktown Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
27041|Cooktown Granite|42369|3|Fully described|p50|Late Permian||Previously mapped as Findlayson Granite.||||||
27041|Cooktown Granite|42474|5|Briefly described|p27|||||||||
27041|Cooktown Granite|43070|2|Defined|p19|Permian||Of Cooktown Supersuite.||||||03-JUN-09
27041|Cooktown Granite|50587|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Geological Province: Kennedy Province.  Fine to medium grained, tourmaline-muscovite-biotite-granite.||||||28-JUN-04
27041|Cooktown Granite|60425|5|Briefly described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Suite (Cooktown Supersuite). S-type. White to pale grey, fine- to medium grained, moderately porphyritic to equigranular (garnet-altered cordierite-) tourmaline-muscovite-biotite granite; miarolitic cavities occur locally.||||||07-FEB-11
27041|Cooktown Granite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
27041|Cooktown Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Suite.|||S-type granitoids.|
27041|Cooktown Granite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Cooktown.||||||
36719|Cooktown Suite|23423|5|Briefly described|Table 7.1 p240|||Of Cooktown Group.||||||
36719|Cooktown Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Early Permian|Of Cooktown Supersuite. Contains the Cooktown, Charlotte and Finch Bay Granites. S-type. Detailed lithology of granites presented in Appdx. 1, p270.||||||07-FEB-11
36719|Cooktown Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Cooktown, Charlotte, Finch Bay Granites.||S-type granitoids.|
75167|Coolah Suite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of the Bedarra Batholith (or Supersuite?). Contains Coolah granite. I-type.||||||07-FEB-11
75168|Coombe granite|60425|6|Mentioned|p98, p288-9 Appdx. |Early Carboniferous|Early Carboniferous|Informal name for a granite on Coombe Island - part of the Bedarra granite belt. Medium- to coarse-grained, slightly to moderately poprhyritic biotite granite; further lithological details presented. I-type.||||||07-FEB-11
24871|Coonambula Granodiorite|23037|4|Described|p43,46,7,8,9,91,135,140|Early Triassic|Late Permian|After Whitaker 1974.  Some sections now mapped as Nogo beds.||||||
24871|Coonambula Granodiorite|33774|3|Fully described|p67|||Contact aureole P28||||||
24871|Coonambula Granodiorite|36333|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic.  Part of the Rawbelle batholith.||||||15-JUL-04
24871|Coonambula Granodiorite|39445|5|Briefly described|Table 12|||||||||
24871|Coonambula Granodiorite|41246|6|Mentioned|Map legend|Triassic|Permian|||||||
24871|Coonambula Granodiorite|43008|5|Briefly described|map legend|||||||||
24871|Coonambula Granodiorite|50598|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Fine grained biotite granodiorite or granite.||||||
24871|Coonambula Granodiorite|61087|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Equigranular, fine-grained biotite granodiorite or granite, irregularly foliated fine to medium-grained biotite gneiss and grey hornblende-biotite granodiorite; common pegmatite and aplite dykes.||||||
24871|Coonambula Granodiorite|61777|5|Briefly described|p227, p225 Tab. 1|||Age: ca 320Ma (SHRIMP U/Pb). Deformed (gneissic) biotite granite.||||||07-FEB-11
24871|Coonambula Granodiorite|64399|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Gneiss and grey hornblende-biotite granodiorite; common pegmatite and aplite dykes.equigranular, fine-grained biotite granodiorite or granite, irregularly foliated fine- to medium-grained biotite gneiss.||||||19-MAR-13
24871|Coonambula Granodiorite|65388|1|Redefined|p285-287, 295, 39, 41, 265, 235, 236|Early Permian|Carboniferous|Of Coonambula Suite. May include McKonkey Granodiorite. In contact with hornfelsed Permian Nogo beds but hornfelsing from Widbury Granite. Intruded by Boolgal Granophyre. Age uncertain. K-Ar age (247 Ma) probably reset. SHRIMP dating of inherited zircon gave ~320Ma. Includes equigranular, fine-grained biotite granodiorite or granite, irregularly foliated fine to medium-grained biotite gneiss, and grey hornblende-biotite granodiorite. See also p247, 296-297, 303-306, 318, 329, 333, 340, 432.||||||
24871|Coonambula Granodiorite|68679|5|Briefly described|p404, p406, p408, p415, p417, p419|Permian|Permian|Auburn Subprovince, New England Orogen. May be part of the same unit with Widbury Granite. Gneissic rocks mapped within the Greystone Granodiorite are probably this unit. Early Permian. Previous K-Ar ages by Webb and McDougall (1968) are probably reset.|~295 Ma (SHRIMP: Fanning et al., 2009).||||Equigranular, fine- to medium-grained saccharoidal biotite granodiorite or granite, moderately to strongly foliated; irregularly foliated fine- to medium-grained biotite gneiss; grey hornblende-biotite granodiorite. Peraluminous S-type.|
24871|Coonambula Granodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Granodiorite.|
77832|Coonambula Suite|65388|5|Briefly described|p295, 281-282, 287, 318, 333,339-340,447|||Rawbelle Batholith. Has some S-type characteristics. Consists of Coonambula , Greystone, Tecoma Granodiorites,  Widbury Granite. ||||||
77832|Coonambula Suite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince. Part of the Rawbelle Batholith.||||||
77832|Coonambula Suite|68679|6|Mentioned|p312, p418-419|Permian|Permian|Northern New England Orogen. Two samples of the Colodon Granodiorite (Wingfield Suite) plot within the Coonambula Suite.||||||
36313|Coonbeta Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36313|Coonbeta Granite|24485|6|Mentioned|p62 Fig.6|||||||||
36313|Coonbeta Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pinkish grey to pale pink, medium-grained, porphyritic (hornblende-)biotite monzogranite.|
36567|Coopers Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 241.  I-Type.||||||
26493|Coorikiana Sandstone|13497|5|Briefly described|p115 fig 6.33, p170, p171|Early Cretaceous|Early Cretaceous|Eromanga Basin. Sandstone were deposited in a shoreface environment. ||Marree Subgroup||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.|Sandstone.|
26493|Coorikiana Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Albian|Albian|In Eromanga Basin.||Of Marree Subgroup||||
26493|Coorikiana Sandstone|22874|6|Mentioned|P18|||||||||
26493|Coorikiana Sandstone|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Oodnadatta Formation, underlying unit is Bulldog Shale||||||
26493|Coorikiana Sandstone|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
26493|Coorikiana Sandstone|23054|5|Briefly described|p21,26,36||Albian|||||||
26493|Coorikiana Sandstone|23056|6|Mentioned|12 table 2|||||||||
26493|Coorikiana Sandstone|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||21-MAY-08
26493|Coorikiana Sandstone|23155|4|Described|p30|Early Cretaceous|Early Cretaceous|Age - Aptian ?(text)     or     Albian ? (diagram)||||||
26493|Coorikiana Sandstone|23375|4|Described|Fig2 p265||Albian|In the Eromanga Basin.||||||21-MAY-08
26493|Coorikiana Sandstone|23982|5|Briefly described|p58 Fig.18|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24175|3|Fully described|p26, p17 Fig. 3|Albian|Albian|Of Marree Group. Conformably overlain by Oodnadatta Sandstone;  transitionally overlies Bulldog Shale.  Max. thickness: 15m.  Geological Province: Eromanga Basin.||||||31-MAR-09
26493|Coorikiana Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|24321|5|Briefly described|Map legend|Albian|Albian|Of the Marree Subgroup.||||||21-MAY-08
26493|Coorikiana Sandstone|30804|6|Mentioned|p10|||||||||
26493|Coorikiana Sandstone|33819|6|Mentioned|p1|||Cretaceous||||||
26493|Coorikiana Sandstone|33822|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
26493|Coorikiana Sandstone|33827|6|Mentioned|p13|||||||||
26493|Coorikiana Sandstone|35002|6|Mentioned|p27|||||||||
26493|Coorikiana Sandstone|38730|6|Mentioned|p29|||||||||
26493|Coorikiana Sandstone|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
26493|Coorikiana Sandstone|39914|6|Mentioned|p3|||||||||
26493|Coorikiana Sandstone|40003|5|Briefly described|Table 15|||||||||
26493|Coorikiana Sandstone|40058|6|Mentioned|p5|||||||||
26493|Coorikiana Sandstone|40199|6|Mentioned|p16|||See also Fig.1||||||
26493|Coorikiana Sandstone|40220|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40670|6|Mentioned|Fig.9|||||||||
26493|Coorikiana Sandstone|40681|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|40910|6|Mentioned|p15|||||||||
26493|Coorikiana Sandstone|40911|6|Mentioned|Map legend|Cenomanian|Cenomanian|Prob. Cenomanian||||||
26493|Coorikiana Sandstone|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|40926|6|Mentioned|p17|||||||||
26493|Coorikiana Sandstone|41060|6|Mentioned|p2|||Generalized stratigraphy. See also Fig.3||||||
26493|Coorikiana Sandstone|41061|6|Mentioned|p9|||||||||
26493|Coorikiana Sandstone|41062|6|Mentioned|Fig.5|||||||||
26493|Coorikiana Sandstone|41064|6|Mentioned|p62|||||||||
26493|Coorikiana Sandstone|41084|5|Briefly described|Fig.2|||||||||
26493|Coorikiana Sandstone|41086|3|Fully described|p98|||||||||
26493|Coorikiana Sandstone|41087|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41088|6|Mentioned|p143|||||||||
26493|Coorikiana Sandstone|41117|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41165|5|Briefly described|p362|||See also Fig.15||||||
26493|Coorikiana Sandstone|41175|6|Mentioned|Fig.1|||||||||
26493|Coorikiana Sandstone|41177|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41182|6|Mentioned|p287|||||||||
26493|Coorikiana Sandstone|41183|6|Mentioned|p307|||||||||
26493|Coorikiana Sandstone|41184|6|Mentioned|p328|||||||||
26493|Coorikiana Sandstone|41187|6|Mentioned|Fig.2|||||||||
26493|Coorikiana Sandstone|41216|6|Mentioned|Fig.18|||||||||
26493|Coorikiana Sandstone|41266|6|Mentioned|Fig.3|||||||||
26493|Coorikiana Sandstone|41523|3|Fully described|p276|||||||||
26493|Coorikiana Sandstone|41535|6|Mentioned|p368|||||||||
26493|Coorikiana Sandstone|41724|6|Mentioned|p383|||||||||
26493|Coorikiana Sandstone|41950|5|Briefly described|Fig.2 P3|||||||||
26493|Coorikiana Sandstone|42071|6|Mentioned|Table 2 P120|||||||||
26493|Coorikiana Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
26493|Coorikiana Sandstone|42293|6|Mentioned|Fig.2 P.18|||||||||
26493|Coorikiana Sandstone|42375|5|Briefly described|Fig.27 P122|Late Cretaceous|Jurassic|Eromanga Basin||||||
26493|Coorikiana Sandstone|42395|5|Briefly described|Fig.13 P83|||||||||
26493|Coorikiana Sandstone|42429|5|Briefly described|p155|||||||||
26493|Coorikiana Sandstone|42520|6|Mentioned|p6|||||||||
26493|Coorikiana Sandstone|42673|6|Mentioned|Fig.5 P189|||||||||
26493|Coorikiana Sandstone|42746|4|Described|p12|||See also Fig.6.||||||21-MAY-08
26493|Coorikiana Sandstone|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||25-MAY-05
26493|Coorikiana Sandstone|43258|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43298|5|Briefly described|Map Legend||Cretaceous|||||||
26493|Coorikiana Sandstone|43591|6|Mentioned|p176|||||||||
26493|Coorikiana Sandstone|43628|6|Mentioned|Fig.3||Early Cretaceous|||||||
26493|Coorikiana Sandstone|43681|5|Briefly described|p296|||||||||
26493|Coorikiana Sandstone|43711|6|Mentioned|p20|||||||||
26493|Coorikiana Sandstone|44133|4|Described|p120-121, 104 Fig 9.11, 117|Late Albian|Middle Albian|Geological Province: Eromanga Basin. Conformably overlies: Bulldog Shale. Formerly a member of the Oodnadatta Formation. Formerly named Attraction Hill Sandstone Member of the Marree Formation. ||||||
26493|Coorikiana Sandstone|44289|5|Briefly described|Map Legend||Albian|||||||
26493|Coorikiana Sandstone|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Bulldog Shale. Overlain by Oodnadatta Formation. Lateral to Toolebuc Formation and Allaru Mudstone; interfingers laterally with Mackunda Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
26493|Coorikiana Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marginal marine sandstone and mudstone.||||||
26493|Coorikiana Sandstone|61312|5|Briefly described|p78, p79 Table E2|Cretaceous|Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Geological Province: Eromanga Basin.||||||
26493|Coorikiana Sandstone|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Of Marree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
26493|Coorikiana Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
26493|Coorikiana Sandstone|63979|6|Mentioned|p48, Fig. 44|Albian|Albian|SA unit that equates to part of the Coreena Member of Wallumbilla Formation in Qld.||||||07-FEB-11
26493|Coorikiana Sandstone|64048|6|Mentioned|p72|||South Australia equivalent to upper part of Wallumbilla Formation in Qld. Geological Province: Cooper Basin. Contains porous sandstones.||||||07-FEB-11
26493|Coorikiana Sandstone|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin. Mis-spelt as Cooriakana in Fig.1c.||Unit in Marree Subgroup.||Underlies Oodnadatta Formation; overlies Bulldog Shale.||10-DEC-15
26493|Coorikiana Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Bulldog Shale. Overlain by Oodnadatta Formation.||||||08-MAR-12
26493|Coorikiana Sandstone|65489|6|Mentioned|p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 20m thick. Hosts gas discovery.  ||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|65925|5|Briefly described|Appendix 2.||||||||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Occurs locally between underlying Bulldog Shale and overlying Oodnadatta Formation.||
26493|Coorikiana Sandstone|66529|6|Mentioned|p12 Fig.5|||||Unit in Neales River Group.||||
26493|Coorikiana Sandstone|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in South Australia.||||
26493|Coorikiana Sandstone|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Sandstone, fine-grained, calcareous, clayey; sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|67462|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|67784|5|Briefly described|p26|Albian|Albian|Southern Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Subsurface only. Shoreface to open marine.||Unit in Marree Subgroup.||Conformably and gradationally overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|Silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|68713|6|Mentioned|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
26493|Coorikiana Sandstone|68715|6|Mentioned|p31 Fig.7|Albian|Albian|||||||
26493|Coorikiana Sandstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (SW). Shallow marine.||Of the Rolling Downs Group.||||
26493|Coorikiana Sandstone|69019|3|Fully described|p85 Fig.21, p97-98.|Albian|Albian|SW Eromanga Basin. Originally defined as a Member of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Type area along Coorikiana Creek, ~40 km SW of Oodnadatta. Thickness varies from <1 to 36 m. Locally an important aquifer.||Unit in Marree Subgroup.||Overlies Bulldog Shale conformably. Is overlain conformably by Oodnadatta Formation.|Coarsening-upwards succession of greenish-white to grey, fine- to very fine-grained sandstone; glauconitic, bioturbated and broadly cross-bedded; sandy siltstone and minor siltstone interbeds; weathers buff to yellow.|
26493|Coorikiana Sandstone|69023|5|Briefly described|p89 Fig.20, p93, p99-100, p102-104, p151|Albian|Albian|See also p191-192. Originally part of Oodnadatta Formation (Freytag, 1966); elevated to Formation status by Thomson (1980). Thickness from <1 to c.35m. Stratigraphic wells intersection data.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation.|A coarsening-upwards succession of greenish-white to grey, glauconitic, bioturbated, cross-bedded fine- to very fine-grained sandstone and silty sandstone; minor siltstone interbeds.|
26493|Coorikiana Sandstone|69457|5|Briefly described|p41:3, 6-8|Early Cretaceous|Early Cretaceous|Thomson (1980); Moore and Pitt (1982). Eromanga Basin. Has not been recognised in the NT; the Wilgunya Subgroup nomenclature is thus preferred to the Marree Subgroup.||Marree Subgroup.||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||12-JUL-16
26493|Coorikiana Sandstone|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Bulldog Shale, overlain by Oodnadatta Formation||
26493|Coorikiana Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
26493|Coorikiana Sandstone|69946|3|Fully described|p21-23, p57, p94, p113-119|Albian|Albian|Moore and Pitt (1982). Previously defined as a Member of Oodnadatta Formation by Freytag (1966), whose type section in Coorikiana Creek, 40km SW of Oodnadatta, still applies. Moore, Pitt et al. (1986) designated a subsurface reference section from 1123 to 1131m in Dullingari 1. Typically <20m thick. Wireline log correlations.||Unit in Marree Subgroup.||Conformably overlies Bulldog Shale. Is overlain conformably by Oodnadatta Formation. Passes laterally into Wallumbilla Formation and Marree Subgroup.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone; minor conglomerate with dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|69947|5|Briefly described|p9, p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin. Shoreline deposits.||Marree Subgroup.||Overlies Bulldog Shale.||
26493|Coorikiana Sandstone|69948|6|Mentioned|Fig.4.1|||Eromanga Basin.||||||
26493|Coorikiana Sandstone|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Fine-grained, calcareous, clayey sandstone; sandy siltstone; minor siltstone.|12-JAN-16
26493|Coorikiana Sandstone|70384|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Eromanga Basin.||Marree Subgroup.||Gradationally overlies Bulldog Shale.|Mostly subsurface: silty fine- to medium-grained sand, broadly cross-bedded, buff to yellow.|
26493|Coorikiana Sandstone|70821|5|Briefly described|p21 Fig.2.6, p23|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Formation.||
26493|Coorikiana Sandstone|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 20m thick. Deposited in a regressive marine, shoreface environment.||||Overlies the Bulldog Shale. Overlain by the Oodnadatta Formation.||
26493|Coorikiana Sandstone|70860|6|Mentioned|p281|||Great Artesian Basin. Mis-spelled as Coorikianna Sandstone.||||||
26493|Coorikiana Sandstone|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
26493|Coorikiana Sandstone|71321|6|Mentioned|p15, p65|||Of Eromanga Basin.||||||24-OCT-19
26493|Coorikiana Sandstone|71342|3|Fully described|Ch1 p19, Ch4 p8, Ch5 p21-p23|Albian|Albian|Originally defined as a member of the Oodnadatta Formation by Freytag (1966) before being elevated to formation status by Moore and Pitt (1982). A type section in Coorikiana Creek was given by Freytag (1966) and a reference section in Dullingari 11 by Moore, Pitt et al (1986). Outcrop, distribution and wireline log characteristics are discussed. Typically less than 20m thick. Sedimentology is discussed briefly. This unit is interpreted to have been deposited in a regressive marine, shoreface environment; however, it should be noted that Alley and White (1996) argue for a middle Albian marine transgressive setting instead. Spore-pollen zone is given in Ch5 p57 and elaborated on in Ch6 p9. Hosts commerically producible oil in Ulandi 12. See also Ch5 p33, Ch5 p57, Ch5 p114-p120, Ch6 p9-p10, Ch7 p10, Ch7 p13, Ch9 p4, Ch9 p9, Ch9 p11, Ch11 p2, Ch11 p5, Ch13 p2.||Marree Subgroup||Conformably overlies the Bulldog Shale. Conformably overlain by the Oodnadatta Formation. Laterally equivalent to the Wallumbilla Formation.|Fine-grained, silty, glauconitic, feldspathic and lithic sandstone with minor conglomerate and dark grey siltstone and mudstone interbeds at the base.|
26493|Coorikiana Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.||Overlies Bulldog Shale. Is overlain by Oodnadatta FZ.||
26493|Coorikiana Sandstone|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet. |||||Sandstone, fine-grained, calcareous, clayey sandy siltstone; minor siltstone.|
26493|Coorikiana Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains gas.||||||
26493|Coorikiana Sandstone|73249|4|Described|p316-319, p320 Fig.2, p321-324, p326-338|Albian|Albian|Eromanga Basin. Early Albian age. Deposited during a partial marine regression to the southwest of the basin, subtidal to beach and fluvial environment. Typically 20m thick. Dominant clay mineral is montmorillonite, deposited in a more arid, warmer envionment than the Cadna-owie Formation. Unit described as sandstone dominated by other authors (Cotton et al., 2006; van der Weilen et al., 2011) but is mostly clay-rich in the samples studied. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks. [Specific locations in text include p324 Fig.4, p334 Tb.7 and p337 Fig.9.]. See also misspelling Coorkiana Sandstone p322.||||Conformably overlies the Bulldog Shale, conformably underlies the Oodnadatta Formation, lateral equivalent of the Toolebuc Formation.|Sandstone with interbedded siltstone and mudstone, typically 20m thick.|
26493|Coorikiana Sandstone|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Contains[?] gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin. Hosts gas.||||Underlain by Bulldog Shale. Overlain by Oodnadatta Formation. Equivalent to Wallumbilla Formation.||
26493|Coorikiana Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p175|Cretaceous|Cretaceous|Eromanga Basin. Shoreface depositional environment.|ca 105 Ma|||Overlies Bulldog Shale, underlies Oodnadatta Formation||
36306|Cope Granite|23510|5|Briefly described|Map Legend||Silurian|of White Springs Supersuite.||||||
36306|Cope Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
36284|Copper Bush Granite|23291|5|Briefly described|p97 Tb. 3.11|Early Permian|Early Permian|Parent: Kangaroo Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
36284|Copper Bush Granite|23510|5|Briefly described|Map Legend||Early Permian|of Kangaroo Creek Supersuite.||||||
36284|Copper Bush Granite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Kangaroo Creek Supersuite.||||
75360|Copper Valley Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite.|||Pink, fine to medium-grained, equigranular biotite granite|
75360|Copper Valley Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Pink, fine- to medium-grained, equigranular biotite granite.|
41794|Coppermine Andesite|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Greenish grey, crystal rich, moderatly lithic, andesitic tuff; some lava and volcaniclastic sandstone.||||||29-SEP-04
41794|Coppermine Andesite|61035|4|Described|p8|Early Permian|Late Carboniferous|Of the Lizzie Creek Volcanic Group. Underlain by Macksford Andesite. Age: ~296Ma (Brich, 1999). Consists of andesitic volcaniclastic arenite, possible with some lava. Geological Province: Connors Sudprovince.||||||07-FEB-11
41794|Coppermine Andesite|65388|3|Fully described|p113-115; p86, 114, 85, 86, 110, 111|Early Permian|Early Permian|Of Lizzie Creek Volcanic Group. Previously informally, the "Coppermine Tuff or Andesite" of Dear (1994a,b, 1995); Defined herein. Macksford Volcanics underlies? Mount Benmore Volcanics overlies? Overlies Leura Volcanics, South Creek Diorite. SHRIMP age: 296.6+/- 2.5Ma. Crystal-rich, lithic-poor andesitic volcaniclastics, massive andesite to dacite. See also p121, 123, 124, 143.||||||
41794|Coppermine Andesite|68679|4|Described|p355, p357-358|||Dear (1994); Withnall et al. (2009). Connors Subprovince. 150m thick. Can be traced 4km along strike.|297 +/- 2.5 Ma (Burch, 1999).|Basal Lizzie Creek Volcanic Group.||Unconformably overlies Macksford Andesite (Leura Volcanics) and South Creek Diorite. Is overlain by Mount Benmore Volcanics.|Massive, unbedded andesite with up to 20% distinctive phenocrysts of greenish yellow, partly altered plagioclase and less abundant altered hornblende crystals; sparse clasts of porphyritic andesite suggest it is mainly volcaniclastic.|
41794|Coppermine Andesite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|297+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Andesite.|
31366|Coppermine Creek Granodiorite|22845|6|Mentioned|Fig6|||||||||
31366|Coppermine Creek Granodiorite|22846|6|Mentioned|p19,20,69|Early Permian|Silesian|4 bodies with a total area of 5 square km.||||||
31366|Coppermine Creek Granodiorite|23608|4|Described|p50 Fig 1||Carboniferous|Also see p51 Fig 3 and p51. I-type intrusion.||||||
31366|Coppermine Creek Granodiorite|43588|6|Mentioned|p30|Late Permian|Late Carboniferous|Variation on Coppermine Creek Granite||||||
31366|Coppermine Creek Granodiorite|44923|5|Briefly described|Map Legend||Carboniferous|||||||
31366|Coppermine Creek Granodiorite|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||28-MAY-04
31366|Coppermine Creek Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Capsize Creek Complex; the Claddagh, Gallangowan, Karandah and Yabba Creek Granodiorites, are all mapped under the same symbol, Cgd.||||||
31366|Coppermine Creek Granodiorite|68679|5|Briefly described|p325-326, p328, p403, p405|Late Carboniferous|Late Carboniferous|Kilkivan-Manumbar area, North D'Aguilar Subprovince. Syntectonic granitoids.||||Intrudes Wongella Metamorphics.|Leucocratic, fine to coarse, subequigranular, pervasively-altered pyroxene-hornblende-biotite granodiorite.|
33154|Copperville Granodiorite|60481|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Grey, medium grained biotite hornblende granodiorite, biotite hornblende quartz diorite and porphyritic microdiorite.||||||
33154|Copperville Granodiorite|61035|5|Briefly described|p17 Tb. 2|Triassic|Permian|Intrudes Glenprairie beds and Rookwood Volcanics; locally affected by deformation associated with the Marlborough Thrust. Age: 255+/-5Ma (isotopic age). Biotite-hornblende granodiorite, biotite-hornblende quartz diorite and porphyritic microdiorite.||||||07-FEB-11
33154|Copperville Granodiorite|65388|2|Defined|p428-429, p70 Fig. 28|Early Triassic|Late Permian|Along with Aitken Creek Gabbro, has horfelsed the Glenprairie beds. In contact with the Aitken Creek Gabbro. K-Ar ages range from 243+/-5 Ma to 250+/-5Ma but may be reset. Includes  grey, medium-grained, equigranular, hornblende-biotite granodiorite, quartz diorite or diorite and porphyritic microdiorite in type area.||||||
33154|Copperville Granodiorite|68359|6|Mentioned|p8|Early Triassic|Permian|||||Intrudes Glenprairie beds.||
33154|Copperville Granodiorite|68679|5|Briefly described|p308, p426|||Yarrol Province. A 2.3 km2 unit on the SW margin of the Aitken Gabbro. K-Ar (biotite/hornblende) ages on 3 samples by Webb and McDougall (1968).|250 +/- 5 Ma to 243 +/- 5 Ma.|||Intrudes Glenprairie beds.|Biotite-hornblende granodiorite, biotite-hornblende quartz diorite; also porphyritic microdiorite.|
75060|Coquelicot Tonalite|64851|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Grey, weakly foliated, medium- to coarse-grained, equigranular hornblende-biotite tonalite; minor fine-grained diorite to tonalite; strong magnetic response.||||||10-FEB-09
75060|Coquelicot Tonalite|68731|5|Briefly described|p123 Fig 3.10, p128, p132, p167|Middle Ordovician|Early Ordovician|Anakie Province. Some outcrops have a weak but distinct foliation that mainly strikes north-northeast. Geochronology from OZCHRON database; Black (pers. Comm. 2004).|471.7 +/- 3.6 Ma |||Intrudes the Les Jumelles beds. Overlain by the Saint Anns Formation.|I-type granite consisting dominantly of grey, fine to coarse grained, equigranular, biotite-hornblende tonalite and quartz diorite.|03-JUL-14
75060|Coquelicot Tonalite|68900|2|Defined|p1, p4, p15, p18-p20|Middle Ordovician|Early Ordovician|Named for Coquelicot Creek, a tributary of the Suttor River. Originally mapped by Olgers (1970) as an unnamed possibly Carboniferous granite pluton. Current mapping [this volume] identified 3 elongate plutons sepereated by Les Jumelles beds. A type locality is designated at 489550 7662650. Outcrop is very poor, however gently undulating topography and reddish loam clearly identify extent of the unit on aerial photographs and Landsat images. Plutons are recognised in geophysics by their magnetic responses. Radiometric responses of plutons are quite variable. Petrography is described.|471 +/- 3.6 Ma (OZCHRON, L.P. Black, pers. comms)|||Intrudes the Les Jumelles beds. Unconformably overlain by the Saint Anns Formation.|Grey, weakly-foliated, fine- to medium-grained, equigranular hornblende-biotite tonalite.|
75060|Coquelicot Tonalite|69541|5|Briefly described|p645 Fig.1(b), p654|Middle Ordovician|Early Ordovician|Thomson Orogen.|471 +/- 4 Ma.|||Intrudes Les Jumelles beds.||
75060|Coquelicot Tonalite|69952|5|Briefly described|p108|||Age determination by Black (pers. comm., in Fergusson and Withnall, 2013).|471 +/- 4 Ma.|||Intrudes Les Jumelles beds.||
75060|Coquelicot Tonalite|70033|6|Mentioned|p1, p18|Early Ordovician|Early Ordovician||471.7 +/- 3.6 Ma, GA sample number 1574649|||||16-JUL-15
75060|Coquelicot Tonalite|70499|5|Briefly described|p6-7|Ordovician|Ordovician|Geological province: Anakie Inlier, Thomson Orogen. Analysis of 5 zircons yield (U-Th)/He ages that range from 208 to 292 Ma, and U-Pb SHRIMP age of 471+\-3.6 Ma (Blake et al., 2012).||||Intruded into Anakie Metamorphic Group.||
75060|Coquelicot Tonalite|70740|4|Described|i, ii, p1, p8, p9, p20-p23|Middle Ordovician|Early Ordovician|Drummond Basin, Anakie Inlier. Defined as basement in the Drummond Basin. Name derived from Coquelicot Creek. Distribution, geophysical response and petrography are discussed. A type locality is designated and briefly described. SHRIMP age derived from Black (unpublished), Easting and Northing for sample are provided.|471.1 +/- 3.6 Ma (SHRIMP U-Pb)|||Intrudes the Les Jumelles beds. Unconformably overlain by the Saint Anns Formation.|Grey, weakly foliated, fine to medium-grained, equigranular hornblende-biotite tonalite with sporadic mafic enclaves.|
75060|Coquelicot Tonalite|70744|5|Briefly described|p939|||Anakie Province.|c.471 Ma (estimated from Fig.7).|||||
75060|Coquelicot Tonalite|70749|5|Briefly described|p43, p48, p54|Ordovician|Ordovician|Anakie Province.|471.7 +/- 3.6 Ma.|||Intrudes the Les Jumelles Beds.||
75060|Coquelicot Tonalite|71966|5|Briefly described|p988-993,996,1000,1002,1004|Early Ordovician|Early Ordovician|Geological province: Anakie Province, Thomson Orogen. Magmatism associated with the 490-460 Ma Larapinta extensional event. Sample 1574649 (outcrop) yielded weighted mean 206Pb/238U age of 471.0+\-3.8 Ma, interpreted as crystallisation age of the rock. Interpreted to be part of a broader suite of Early Ordovician magmatism within in the Thomson Orogen, which includes the I- and S-type intrusive magmatism of the Charters Towers and Lolworth batholiths (northeastern Thomson Orogen; Fergusson et al., 2013), S-type magmatism in the Anakie Province,  and I-type tonalite and granites in the Greenvale Province and surrounds. Synchronous with widespread turbidite deposition e.g. Warratta Group (Greenfield et al., 2010) and Thomson beds (Purdy et al., 2016b).|471+\-3.8 Ma (crystallisation)||||Biotite hornblende tonalite.|25-OCT-19
75060|Coquelicot Tonalite|73425|6|Mentioned|p16|Middle Ordovician|Middle Ordovician|Anakie Province, northeast Thomson Orogen.||||||
73023|Coral Gardens Formation|63152|5|Briefly described|p120 Fig. 3|||Of the Jack Group (Graveyard Creek Supergroup). Overlies Red Bull Formation; overlain by Jack Hills Limestone. Thin limestone passing up into oncolitic and oolitic limestones.||||||10-APR-07
27285|Corbett Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Mount Norna Quartzite.||||||07-NOV-08
27285|Corbett Formation|23032|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27285|Corbett Formation|23220|5|Briefly described|Fig.2|||of Robertson River Subgroup.||||||
27285|Corbett Formation|23291|4|Described|p23, p85 Tb 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Geological Province: Georgetown Region.||||||18-MAY-15
27285|Corbett Formation|38714|2|Defined|p188|Mesoproterozoic|Mesoproterozoic|||||||
27285|Corbett Formation|38715|6|Mentioned|p191|||||||||
27285|Corbett Formation|39495|6|Mentioned|p142|||||||||
27285|Corbett Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27285|Corbett Formation|39924|6|Mentioned|p341|||||||||
27285|Corbett Formation|41975|6|Mentioned|p435|||||||||
27285|Corbett Formation|42199|5|Briefly described|Table 1 P280|||||||||
27285|Corbett Formation|43664|4|Described|p25-27|||||||||
27285|Corbett Formation|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
27285|Corbett Formation|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group). Includes the Tin Hill Quartzite Member.||||||18-MAY-15
27285|Corbett Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Overlies: Dead Horse Meatbasalt. Intruded by Cobbold Metadolerite. Underlies: Lane Creek Formation.||||||18-MAY-15
27285|Corbett Formation|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group). Overlies Dead Horse Metabasalt. Conformably overlain by Lane Creek Formation. Intruded by Cobbold Metadolerite.||||||07-NOV-08
27285|Corbett Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||19-AUG-04
27285|Corbett Formation|50595|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Overlies: Daniel Creek Formation. Underlies: Lane Creek Formation.||||||18-MAY-15
27285|Corbett Formation|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
27285|Corbett Formation|65887|5|Briefly described|p41|Paleoproterozoic|Statherian|Of Robertson River Subgroup. Overlies Dead Horse Metabasalt. Overlain by Lane Creek Formation.||||||
27285|Corbett Formation|66800|5|Briefly described|p926 Table 1, p928|||||Unit in Robertson River Subgroup.||Overlies Dead Horse Metabasalt. Is overlain by Lane Creek Formation.||
27285|Corbett Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier.|~1660-1650 Ma.|Lower Etheridge Group.|||Mudstone.|
27285|Corbett Formation|67341|5|Briefly described|vi, p10-13|||Forsayth Subprovince, Etheridge Province.|1791 +/- 10 Ma (SHRIMP U-Pb zircon).|||Overlies Dead Horse Metabasalt. Is overlain by Lane Creek Formation.|Includes calcareous, fine- to coarse-grained, occasionally thick-bedded sandstones with fine-grained, thinly-bedded, laminated siltstones.|
27285|Corbett Formation|67430|6|Mentioned|p25|||||||||
27285|Corbett Formation|68352|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Conformably overlies Daniel Creek Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Lane Creek Formation.|Mica schist (+/- staurolite, andalusite, sillimanite, garnet).|
27285|Corbett Formation|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.|Includes Tin Hill Quartzite Member.|Conformably overlies Dead Horse Metabasalt. Is intruded by Cobbold Metadolerite. Is overlain conformably by Lane Creek Formation.|Mica schist (+/- staurolite, andalusite, sillimanite, garnet); grades into green-grey mudstone (+/- chloritoid); quartzite.|
27285|Corbett Formation|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Is intruded by Cobbold Metadolerite. Is overlain conformably by Lane Creek Formation.|Mica schist (+/- staurolite, andalusite, sillimanite, garnet).|
27285|Corbett Formation|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Conformably overlies Dead Horse Metabasalt. Is intruded by Cobbold Metadolerite. Is overlain conformably by Lane Creek Formation.|Greenish-grey mudstone (+/- chloritoid); lesser quartzite.|
27285|Corbett Formation|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes a separately mapped facies variant. Contains thin bands of white quartzite.||Of the Robertson River Subgroup.||Intruded by the Cobbold Metadolerite. Conformably overlies Dead Horse Metabasalt. Is overlain conformably by Lane Creek Formation.|Greenish grey mudstone (+/- chloritoid), grades into mica schist (+/- staurolite, andalusite, sillimanite, garnet); mica schist (+/- staurolite, andalusite, sillimanite, garnet), grades into green-grey mudstone (+/- chloritoid).|
27285|Corbett Formation|68576|6|Mentioned|Q_11: p24|||Georgetown area.||||||
27285|Corbett Formation|69582|6|Mentioned|p76|||Etheridge Province. Intersected in GSQ Georgetown 8-9R.||Robertson River Subgroup||||
27285|Corbett Formation|69591|4|Described|p61-64, p68, p108|Paleoproterozoic|Paleoproterozoic|Forsayth Subprovince, Etheridge Province. The schist facies of this unit closely resembles the Juntala Metamorphics. Up to 1000m thick. Comagmatic with Cobbold Metadolerite. Detrital zircon spectra.|~1785 Ma.|Robertson River Subgroup.|Tin Hill Quartzite Member.|Overlies Dead Horse Metabasalt.|Mainly deepwater mudstone. The lower part is slightly carbonaceous and laminated, passing upwards into a monotonous succession of relatively massive mudstone or phyllite, locally with chloritoid porphyroblasts; grades into mica schist to the E.|
27285|Corbett Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1791+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
27285|Corbett Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Georgetown area.|ca 1675-1650 Ma|||Overlies the Dead Horse Metabasalt.|Siltstone, carbonaceous shale and dolomite.|03-OCT-18
27285|Corbett Formation|72297|6|Mentioned|p728|||Etheridge Province. A minor source of slate; quarries in the Forsayth area.||||||
27285|Corbett Formation|72983|6|Mentioned|p70|Statherian|Orosirian|Date is a maximum depositional age from Neumann and Kositcin (2011).|1791 +/- 10 Ma|||||
36297|Corduroy Swamp Granite|23291|6|Mentioned|p40|||See also Corduroy Swamp granite. Geological Province: Georgetown Region.||||||08-JUL-15
36297|Corduroy Swamp Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
34130|Cornelia Orthogneiss|22630|4|Described|p40|||||||||
34130|Cornelia Orthogneiss|22844|4|Described|Fig4 p21,40-42|Ordovician|Cambrian|Intrudes Cape River Metamorphics.||||||
34130|Cornelia Orthogneiss|23283|2|Defined|p26|Ordovician|Cambrian|||||||
34130|Cornelia Orthogneiss|23422|5|Briefly described|p212 Table 6.7|||||||||
34130|Cornelia Orthogneiss|23508|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
34130|Cornelia Orthogneiss|68731|5|Briefly described|p136, p147|Middle Ordovician|Early Ordovician|Geochronology by Wormald (unpublished data). Mapped as a discrete body.|472.1 +/- 6.1 Ma, U-Pb zircon (LA-ICP-MS)|||Intrudes the Cape River Metamorphics.||
36522|Cornstalk tonalite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 173.||||||
23513|Coteeda Subgroup|40090|6|Mentioned|p83|||||||||
23513|Coteeda Subgroup|40091|5|Briefly described|p72|||||||||
23513|Coteeda Subgroup|40093|6|Mentioned|Table 1|||||||||
23513|Coteeda Subgroup|40954|6|Mentioned|p132|||||||||
23513|Coteeda Subgroup|41546|4|Described|p157|||||||||
23513|Coteeda Subgroup|41666|6|Mentioned|Fig.1|||||||||
38880|Coulston Volcanics|24489|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38880|Coulston Volcanics|24615|5|Briefly described|CD|Early Triassic|Early Triassic|[Rvc].  Aphyric to porphyritic dacite, locally flow banded and autobrecciated; welded crystal-poor dacitic ignimbrite.||||||10-APR-13
38880|Coulston Volcanics|65452|5|Briefly described|p5-8, p35|||Southern Yarrol Province. Crops out in a small area around Mount Coulston. Possibly equivalent to Agnes Water Volcanics: similar geochemistry.|||||Mafic to intermediate volcaniclastic and coherent deposits.|
38880|Coulston Volcanics|68008|4|Described|p199-201, p209, p326, p329|Late Triassic|Late Triassic|New unit; type area is along the S side of Mount Coulston, N of Woodside homestead. Has an arcuate outcrop 3.5 km x 2 km. Up to 400m thick. Geochemistry described; similarities with some Winterbourne Volcanics rhyolites.||||Overlies Miriam Vale Granodiorite. Correlated with Winterbourne Volcanics.|Mainly trachyandesite to trachydacite, locally flow-banded and autobrecciated, with some welded crystal-poor ignimbrite; locally more mafic, including intermediate to basic coarse breccias.|
38880|Coulston Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
38880|Coulston Volcanics|68679|5|Briefly described|p312-313, p442|Late Triassic|Late Triassic|Agnes Water-Biloela region, northern New England Orogen.|||||Autobrecciated basaltic to andesitic lava, coherent and autobrecciated porphyritic dacite, and crystal-poor dacitic ignimbrite.|
27951|Cowie Granite|23967|6|Mentioned|p1331|||Geological Province: Williams batholith.||||||
27951|Cowie Granite|24197|6|Mentioned|p96 Tb. 12.1|||Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
27951|Cowie Granite|37862|4|Described|p588|||||||||
27951|Cowie Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27951|Cowie Granite|38658|6|Mentioned|p152|||||||||
27951|Cowie Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
27951|Cowie Granite|39445|6|Mentioned|Table 2|||||||||
27951|Cowie Granite|40840|6|Mentioned|Map legend|||||||||
27951|Cowie Granite|41306|5|Briefly described|p13|||Mention p4.||||||15-MAR-07
27951|Cowie Granite|42556|5|Briefly described|Fig.2 P4|||||||||
27951|Cowie Granite|45161|5|Briefly described|p51|||See also p52.||||||15-MAR-07
27951|Cowie Granite|45166|5|Briefly described|p38|||||||||
27951|Cowie Granite|49009|2|Defined|p11|Proterozoic|Proterozoic|Mapped as Williams Granite (Carter and Opik 1963)||||||15-MAR-07
27951|Cowie Granite|49041|5|Briefly described|Table 3|||||||||
27951|Cowie Granite|50100|5|Briefly described|p21|Calymmian|Calymmian|Of the Maramungee Suite.||||||
27951|Cowie Granite|50536|5|Briefly described|p1.5 Table 1.1|||Geological Province: Mount Isa Inlier.  Of the Cowie Suite.||||||
27951|Cowie Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Leucocratic granodiorite, granite, tonalite.||||||
27951|Cowie Granite|65396|6|Mentioned|p360|||Cloncurry District.|~1550 Ma|||||
33046|Cowie Suite|50536|5|Briefly described|p1.5, 11.3, Table 1.1|||Geological Province: Mount Isa Inlier.||||||
33046|Cowie Suite|67323|5|Briefly described|GIS attrib tbl; p21|Mesoproterozoic|Mesoproterozoic|Wyborn et al. (2001). Williams Igneous Event.||Williams Supersuite.|?Boorama Tank Gneiss.|Intrudes Soldiers Cap Group and Staveley Formation.|Granodiorite, pegmatite, leucocratic tonalite.|
33046|Cowie Suite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.|||Boorama Tank Gneiss|||05-MAY-16
33046|Cowie Suite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Boorama Tank Gneiss.|||
33046|Cowie Suite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Blackeye Granite.||Granodiorite, pegmatite, leucocratic tonalite.|20-JAN-22
33046|Cowie Suite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Blackeye Granite.||Granodiorite, pegmatite, leucocratic tonalite.|
36190|Cowley Ophiolite Complex|23497|5|Briefly described|Table 1||Neoproterozoic|||||||
36190|Cowley Ophiolite Complex|23507|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|||||||
36190|Cowley Ophiolite Complex|60425|5|Briefly described|p6, p107|||Consists of metamorphosed serpentinite, talc schist, (talc-)tremolite schist, (tremolite-) chlorite schist and talc-mgnesite rocks containing relict peridotite as well as some gabbro, and basaltic or andesitic dykes.||||||07-FEB-11
36190|Cowley Ophiolite Complex|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Barnard Province. This unit, as well as Barnard Metamorphics and Babalangee Amphibolite, are all mapped under the symbol, -Pob.||||||
36190|Cowley Ophiolite Complex|69030|6|Mentioned|p6|Cambrian|Cambrian|Barnard Province.||||||
36190|Cowley Ophiolite Complex|70033|6|Mentioned|p52 Fig 8.1|||Thomson Orogen. Age shown in map legend (Fig 8.1) as Neoproterozoic - Ordovician?||||||
36190|Cowley Ophiolite Complex|73595|6|Mentioned|p1132-1133, 1135-1144|||Situated 20km S of Innisfail, emplaced along the Russell-Mulgrave Fault (an ancient subduction margin). Presented as COC after the first couple of mentions. Lithologies described; photographs, photomicrographs. Geochemistry described in great detail.|||||A differentiated mafic-ultramafic complex composed of gabbro, chlorite schist, antophyllite schist and serpentinite. Reflects an amphibolite facies metasomatic overprint.|
38178|Craigie Supersuite|23422|4|Described|p178, p215 Table 6.9|Early Devonian|Late Silurian|||||||
38178|Craigie Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Deane, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
38178|Craigie Supersuite|69592|5|Briefly described|p280-281,p283,p285,p288-289 Figs.4.84,88|||Reedy Springs Batholith, Charters Towers Province. Geochemistry described; similar to the Dido Supersuite in Georgetown Inlier.|c.406 Ma.||Craigie Tonalite.||Foliated hornblende-biotite and biotite-hornblende tonalite. I-type.|
35048|Craigilee beds|13996|6|Mentioned|p140, p144|||Rockhampton district. Contains Pridoli brachiopods with no sign of regional differentiation, and a few trilobites.||||||
35048|Craigilee beds|23037|6|Mentioned|p23|Devonian|Silurian|||||||
35048|Craigilee beds|23468|6|Mentioned|Table 1 p 296|||||||||
35048|Craigilee beds|24491|4|Described|p16|||||||||
35048|Craigilee beds|24615|5|Briefly described|CD|Early Devonian|Late Silurian|[SDc].  Sandstone, siltstone, mudstone, andesitic to dacitic volcanics, volcaniclastic breccia, limestone, polymictic conglomerate, sparse peperite and andesite to dacite intrusives.||||||
35048|Craigilee beds|50209|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
35048|Craigilee beds|50213|5|Briefly described|Map legend|Early Devonian|Late Silurian|||||||
35048|Craigilee beds|60557|5|Briefly described|p21, p29|Middle Devonian|Late Silurian|See also Craigilea beds (which may be misspelt?).  Includes limestones and arenites, as well as andesites, volcanoclastic sediments, rhyodacites and volcanic sandstones.  Host to auriferous quartz veins. Unconformably overlain by Mount Alma Formation.||||||09-JUN-05
35048|Craigilee beds|61147|5|Briefly described|p376.|Early Devonian|Late Silurian|Oldest rocks in the Dee Range area. Crops out over 190 sq.km.|||||Sandstones, siltstones, and conglomerates as well as dacitic and andesitic volcanic rocks and minor autochthonous limestones.|
35048|Craigilee beds|61730|5|Briefly described|p994 Fig.1, p1000, p1001|Middle Devonian|Late Silurian|Basal sst, siltst, conglomerate with minor limestone; middle section comprises abundant porphyritic intermediate to felsic rocks and high-level intrusions, ripple and cross-laminated sst; top of beds dominated by clastic sediments. Geol Prov: Yarrol Prov.||||||21-APR-06
35048|Craigilee beds|63600|5|Briefly described|p900 Fig. 1, p915|Middle Devonian|Late Silurian|Adjacent to the Princhester Serpetninite.||||||07-FEB-11
35048|Craigilee beds|65388|6|Mentioned|p439|||Part  of a belt of Silurian to early Carboniferous rocks.||||||
35048|Craigilee beds|68008|3|Fully described|p10-18, p22, p26, p89, p109, p113, p131|Middle Devonian|Late Silurian|See also p261, p307, p393, p477, p479, p568-569, p573, p575-577, p600-601. Talent et al. (1982), Bradley (1994). Named after Craigilee homestead, Mount Cassidy area. Composite section by Bradley (1994) has thickness of ~3000m. Crops out as low to moderate hills and strike ridges. Not formally subdivided. Lithologies well-illustrated and described in detail. May correlate with Capella Creek Group. Geochemistry discussed. Fossil species listed. Submarine deposits. Princhester Serpentinite is thrust over this unit. Timing of deformation discussed. Appears as Craigilee Group on p393. Micropaleontology detailed. Coral species listed.||||Is overlain unconformably by Mount Alma Formation and Mount Salmon Volcanics. Is intruded by Ridgelands Granodiorite. Is faulted against Rockhampton Group and Youlambie Conglomerate.|Feldspathic sandstone, siltstone, granule conglomerate, fossiliferous limestone, minor intermediate to felsic volcanic rocks, rare basalt.|
35048|Craigilee beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Marble Waterhole, Calliope, Munbooree and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
35048|Craigilee beds|68679|5|Briefly described|p312-315, p338, p347|Emsian|Emsian|Talent, Berry and Boucot (1982). Northern New England Orogen. Occurs in inliers and fault blocks (the Morinish and Mount Cassidy Belts). Comprises a 2500-3000m thick succession of three informal units (described). Formed in a volcanic arc above a subduction zone. Is partly coeval with the Calliope beds. Age from corals; previously thought to extend back to latest Silurian.|||||Feldspathic sandstone, siltstone, conglomerate, limestone with minor intermediate to felsic volcanics; flow breccia, hyaloclastite, lava, sandstone, mudstone and siltstone; topped by feldspathic sandstone with siltstone, mudstone and conglomerate.|
35048|Craigilee beds|69952|6|Mentioned|p75|Devonian|Late Silurian|||||||23-NOV-15
35048|Craigilee beds|73143|6|Mentioned|p11, p18|Emsian|Emsian|Yarrol Basin. Contains Favosites grandipora tabulate coral and Aphyllum simplexum rugose coral (Blake, 2010).||||||
39082|Craiglands Quartz Monzodiorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Littlemore Suite.  Geological Province: Yarrol Province.||||||
39082|Craiglands Quartz Monzodiorite|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pgcr].  Grey to pink medium-grained hornblende quartz mozodiorite, hornblende-augite quartz diorite, biotite-hornblende quartz diorite.||||||
39082|Craiglands Quartz Monzodiorite|50197|5|Briefly described|Map Legend|Permian|Permian|||||||
39082|Craiglands Quartz Monzodiorite|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Grey to pink, medium-grained hornblende quartz monzodiorite, hornbelnde-augite quartz diorite, biotite-hornblende quartz diorite.||||||18-JUN-09
39082|Craiglands Quartz Monzodiorite|68008|2|Defined|p144-145, p147, p182-184, p334, p367-369|Permian|Permian|See also p375, p380, p383, p484, p528, p624, p626-627. New name, after the property Craiglands. Has two main outcrops (described) separated by the Smoky beds. The type area is a 2km length of Spring Creek upstream from where it is crossed by the station track. Makes up a small part of the Mount Gerard Complex area; the rest is the Smoky beds. Geophysical expression described: strongly magnetic, par of the Marlborough Gravity Ridge. Geophysics modelling. Geochemistry detailed. Comagmatic with Inverness Volcanics. Hosts several small gold deposits.|256.8 +/- 2.6 Ma (U-Pb zircon).|||Intrudes Youlambie Conglomerate and Inverness Volcanics. Intrudes and is partly covered by the Smoky beds.|Grey to pink, medium-grained rocks ranging from quartz gabbro to quartz monzonite; biotite-augite-hornblende quartz monzodiorite and biotite-augite monzogabbro most common. Plagioclase is almost always the main mineral; quartz is always present.|
39082|Craiglands Quartz Monzodiorite|68679|5|Briefly described|p343, p425, p427|||Part of the Mount Gerard Complex (Dear et al., 1971). Surrounds a roof pendant of the Smoky beds. May be comagmatic with the Inverness Volcanics. Geochemistry briefly described.||||Intrudes and is partly overlain by the Smoky beds. Intrudes Youlambie Conglomerate.|Hornblende quartz monzodiorite, hornblende-augite quartz diorite, biotite-hornblende quartz diorite.|
68960|Crane Creek Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey and pink, medium-grained, even-grained, biotite granite.|
68960|Crane Creek Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey and pink, medium-grained, even-grained, biotite granite.|
40849|Cranky Creek Microgranodiorite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
40849|Cranky Creek Microgranodiorite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Grey to pink, porphyritic, biotite and hornblende-biotite microgranodiorite.|
23520|Crimea Granite|22847|3|Fully described|p 40|||||||||
23520|Crimea Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
23520|Crimea Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 115. ?S-Type.||||||
23520|Crimea Granite|42245|2|Defined|p33|Ordovician||||||||
23520|Crimea Granite|43093|4|Described|Appendix 1||Ordovician|Middle Ordovician||||||
23520|Crimea Granite|43259|4|Described|Appendix 1,p23.||Ordovician|||||||
23520|Crimea Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
36372|Crocodile Formation|23425|5|Briefly described|p373 Fig 9.10|||Of Pascoe River Group.||||||
36166|Croissant Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36166|Croissant Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 261. I-Type.||||||
36166|Croissant Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36166|Croissant Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, fine- to medium-grained and pegmatitic, granophyric biotite granite. I-type.||||||07-FEB-11
27755|Cromwell Metabasalt Member|23031|5|Briefly described|24|Paleoproterozoic|Paleoproterozoic|Geol province Mount Isa Fold Belt. Of the Eastern Creek Volcanics.||||||07-NOV-08
27755|Cromwell Metabasalt Member|23395|5|Briefly described|p386 Fig.3|||Of the Eastern Creek Volcanics.||||||15-MAR-07
27755|Cromwell Metabasalt Member|23518|5|Briefly described|p11|Proterozoic|Proterozoic|Of Eastern Creek Volcanics.  Geological Province: Western Fold Belt.||||||
27755|Cromwell Metabasalt Member|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics.  Underlies the Lena Quartzite Member.||||||25-AUG-04
27755|Cromwell Metabasalt Member|30534|2|Defined|p302|Carpentarian|Carpentarian|||||||
27755|Cromwell Metabasalt Member|33900|5|Briefly described|p11|||||||||
27755|Cromwell Metabasalt Member|35295|6|Mentioned|Fig.2|||||||||
27755|Cromwell Metabasalt Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27755|Cromwell Metabasalt Member|38232|6|Mentioned|p84|||||||||
27755|Cromwell Metabasalt Member|38233|5|Briefly described|Table 1|||||||||
27755|Cromwell Metabasalt Member|38234|6|Mentioned|p103|||||||||
27755|Cromwell Metabasalt Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27755|Cromwell Metabasalt Member|38560|6|Mentioned|p114|||||||||
27755|Cromwell Metabasalt Member|39622|6|Mentioned|p30|||See also Appendix||||||
27755|Cromwell Metabasalt Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27755|Cromwell Metabasalt Member|39924|6|Mentioned|p348|||||||||
27755|Cromwell Metabasalt Member|39934|6|Mentioned|p317|||||||||
27755|Cromwell Metabasalt Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27755|Cromwell Metabasalt Member|40221|3|Fully described|p7|||||||||
27755|Cromwell Metabasalt Member|40598|6|Mentioned|Fig.2|||||||||
27755|Cromwell Metabasalt Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
27755|Cromwell Metabasalt Member|41307|4|Described|p9|||||||||
27755|Cromwell Metabasalt Member|42565|6|Mentioned|p8|||Of Eastern Creek Volcanics, Mt. Isa.||||||15-MAR-07
27755|Cromwell Metabasalt Member|42782|6|Mentioned|p463|||Same unit  as Cromwell Metabasalt, Cromwell Member.||||||15-MAR-07
27755|Cromwell Metabasalt Member|45136|4|Described|p47|||||||||
27755|Cromwell Metabasalt Member|45166|5|Briefly described|p15|||||||||
27755|Cromwell Metabasalt Member|46801|6|Mentioned|p123|||||||||
27755|Cromwell Metabasalt Member|47083|5|Briefly described|p5|||Oldest member of Eastern Creek Volcanics (Haslingden Group).||||||15-MAR-07
27755|Cromwell Metabasalt Member|49041|6|Mentioned|Table 4|||||||||
27755|Cromwell Metabasalt Member|50100|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Eastern Creek Volcanics.||||||
27755|Cromwell Metabasalt Member|61204|5|Briefly described|p540|||Geological Province: Mount Isa Inlier. Of the Eastern Creek Volcanics. Greenschist facies metamorphosed interflow sedimentary unit.||||||
27755|Cromwell Metabasalt Member|62873|5|Briefly described|p692, p704-5|Paleoproterozoic|Paleoproterozoic|Of the Eastern Creek Volcanics. Underlies the Lena Quartzite Member. In the Haslingden area this unit dominates the Eastern Creek Volcanics sequence and has undergone greeschist facies metamorphism.||||||07-NOV-08
27755|Cromwell Metabasalt Member|63023|5|Briefly described|p1025 Fig. 2|||Of Eastern Creek Volcanics (Haslingden Group). Geological Province: Leichardt Superbasin.||||||
27755|Cromwell Metabasalt Member|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Eastern Creek Volcanics. Overlain by Lena Quartzite Member. Geological Province: Leichhardt Superbasin. Tholeiitic mafic intrusions comprising metabasalts, sediments and tuffs.||||||07-FEB-11
27755|Cromwell Metabasalt Member|64367|5|Briefly described|p555  Fig. 1b|Paleoproterozoic|Paleoproterozoic|See also Pickwick Member. The abbreviated version of the name is used throughout the text - all relevant details are therefore attached to that version of the name. Of Eastern Creek Volcanics.||||||07-FEB-11
27755|Cromwell Metabasalt Member|64832|5|Briefly described|p1153, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Lower member of the Eastern Creek Volcanics. Ages: 1807+/-78Ma and 1710+/-25Ma. Geological Province: Mt Isa Inlier. Has high titanium conten - detailed geochemistry included. Referred to throughout paper.||||||07-FEB-11
27755|Cromwell Metabasalt Member|64834|5|Briefly described|p15|||Leichhardt Superbasin. Western Succession of Mount Isa Basin. Mentioned in result figures as Cromwell sediments.||Lower part of Eastern Creek Volcanics||Is overlain by Lena Quartzite.||
27755|Cromwell Metabasalt Member|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p13|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl. Leichhardt Superbasin.||Eastern Creek Volcanics.||Is overlain by Lena Quartzite Member.|Metabasalt, amygdaloidal metabasalt, flow-top breccia, tuff.|
27755|Cromwell Metabasalt Member|67499|6|Mentioned|p938|||||Of the Eastern Creek Volcanics.||||08-MAY-12
27755|Cromwell Metabasalt Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
27755|Cromwell Metabasalt Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Dynamite Creek Member. Is overlain by Lena Quartzite Member.|Metabasalt (locally amygdaloidal), flow-top breccia and tuff. (Separately mapped) feldspathic sandstone, epidote sandstone, quartzite and conglomerate.|
27755|Cromwell Metabasalt Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Dynamite Creek Member. Is overlain by Lena Quartzite Member.|Metabasalt (locally amygdaloidal), flow-top breccia and tuff. (Separately mapped) feldspathic sandstone, epidote sandstone, quartzite and conglomerate.|
27755|Cromwell Metabasalt Member|71799|4|Described|p150 fig 2, p152|Statherian|Statherian|Lawn Hill. Erupted in a subaerial environment dominated by braided river systems. Flows are between 1 and 140m thick. Provisionally correlated with the Magna Lynn Metabasalt. See also p153 tbl 1, p156, p157-p158.|ca. 1775 Ma|Eastern Creek Volcanics||Overlies the Mount Guide Formation. Overlain by the Lena Quartzite Member.|Basaltic lava flows that are typically rubbly to vesicular at the tops.|03-OCT-18
27755|Cromwell Metabasalt Member|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Eastern Creek Volcanics|||metabasalt; fluviolacustrine sandstone between basalt flows.|
27755|Cromwell Metabasalt Member|73553|5|Briefly described|p231|||Western Succession.||Eastern Creek Volcanics||||
27382|Crooked Creek Conglomerate|23032|4|Described|p21,22||Early Silurian|||||||
27382|Crooked Creek Conglomerate|23424|5|Briefly described|Table 8.1 p333||Early Silurian|Thickness: At least 300 m underlies type section of Quinton Formation. Is the basal unit of the Graveyard Creek Group and unconformably overlies Judea Fm and Gray Creek Complex. Of Graveyard Creek Group, Graveyard Creek Subprovince.  Maximum Thickness 300||||||
27382|Crooked Creek Conglomerate|23430|5|Briefly described|p476|||Underlying Unit Quinton Formation. Broken River Province.||||||
27382|Crooked Creek Conglomerate|24577|4|Described|p752 Fig. 1|Silurian|Silurian|Overlain by the Quinton Formation. Overlies the Carriers Well Formation"" and the Wairuna Formation. Conglomerate is Cong. in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
27382|Crooked Creek Conglomerate|31999|6|Mentioned|p139|||Table 11||||||
27382|Crooked Creek Conglomerate|41260|3|Fully described|p36|||Described p145.||||||07-MAY-15
27382|Crooked Creek Conglomerate|41679|6|Mentioned|Fig.2|||||||||
27382|Crooked Creek Conglomerate|41719|1|Redefined|p217|Silurian||||||||
27382|Crooked Creek Conglomerate|42032|6|Mentioned|Fig.2 P488|||||||||
27382|Crooked Creek Conglomerate|42054|6|Mentioned|p273|||||||||
27382|Crooked Creek Conglomerate|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27382|Crooked Creek Conglomerate|42933|1|Redefined|p55|Early Silurian|Late Ordovician|Of the Graveyard Creek Group.||||||10-APR-08
27382|Crooked Creek Conglomerate|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Graveyard Creek Group.||||||
27382|Crooked Creek Conglomerate|43664|6|Mentioned|p83|||||||||
27382|Crooked Creek Conglomerate|45009|14|Not recorded|p102|Early Devonian|Late Silurian|||||||
27382|Crooked Creek Conglomerate|67848|4|Described|p14.|Early Silurian|Early Silurian|Basal unit in the cover sequence of Broken River Province. Submarine mass flow deposits from 300 m to 1 km thick. Contains substantial limestone olistoliths to 2 km long, possibly from Carriers Well Formation.|c.435 Ma.|Basal unit in Graveyard Creek Group.||Is overlain conformably by Quinton and Poley Cow Formations.|Contains pebble to boulder clasts of (Judea Formation) sandstone, granitoid and mafic-ultramafic rocks, basalt and limestone; matrix sands are locally rich in amphibole.|
27382|Crooked Creek Conglomerate|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince. Separately mapped is an un-named facies of limestone (calcarenite, calcilutite, calcirudite), locally bioclastic, probably mainly olistoliths.||Unit in Graveyard Creek Group.|||Polymictic pebble to boulder conglomerate, feldspatholithic sandstone and minor mudstone; local large olistoliths of limestone, amphibolite and schist.|
27382|Crooked Creek Conglomerate|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince. Separately mapped is an un-named facies of limestone (calcarenite, calcilutite, calcirudite), locally bioclastic, probably mainly olistoliths.||Unit in Graveyard Creek Group.|||Polymictic pebble to boulder conglomerate, feldspatholithic sandstone and minor mudstone; local large olistoliths of limestone, amphibolite and schist.|
27382|Crooked Creek Conglomerate|68731|6|Mentioned|p157|Silurian|Silurian|Graveyard Creek Subprovince (Arnold and Henderson 1976; Henderson 1987; Withnall and Lang 1993).||||||
27382|Crooked Creek Conglomerate|69030|5|Briefly described|p6|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province).||Graveyard Creek Group||||
27382|Crooked Creek Conglomerate|69592|4|Described|p259-262, p267|Early Devonian|Silurian|Graveyard Creek Subprovince, Broken River Province. Thickness ranges from >300m to perhaps 600m (in the N), to 5-15m in the S where it had been included in the Poley Cow Formation (Fielding cited in Withnall et al., 1993). Rapid mass flow deposition in submarine fans.||Basal Graveyard Creek Group.||Unconformably overlies Judea Formation. Is overlain conformably by Poley Cow or Quinton Formations.|Massive, poorly-sorted, polymict, boulder to pebble conglomerate; mainly clast-supported; clasts (up to 30cm diameter) generally rounded to subangular; matrix mainly sand, some mud; rare sandstone stringers; two micritic limestone lenses to 2km long.|
28022|Crosbie Formation|23420|5|Briefly described|p 142 table 4.4 + p 123|||In the Edward River Metamorphic Group, of the Savannah Province. Thickness >500m||||||
28022|Crosbie Formation|43596|4|Described|p16, p20 Tb. 1||Proterozoic|Of the Edward River Metamorphic Group. Conformable over O'Lane Formation. Max. thickness: 600m. Predominantly light grey to pinkish grey, generally fine-grained and saccharoidal orthoquartzite, which contains minor muscovite or sericite - more lith detail.||||||07-APR-15
28022|Crosbie Formation|69591|5|Briefly described|p78 Tb.2.6|sw||Savannah Province, Coen Inlier. >500m thick; top not exposed.||Edward River Metamorphic Group.|||Mostly well-bedded quartzite.|
26505|Crown Point Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Pedirka Basin||||||
26505|Crown Point Formation|22566|5|Briefly described|p79|Early Permian|Late Carboniferous|Of the Finke Group.||||||08-AUG-06
26505|Crown Point Formation|22804|6|Mentioned|p455||Early Permian|||||||
26505|Crown Point Formation|22824|6|Mentioned|p537||Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22826|4|Described|p576|Early Permian|Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22883|6|Mentioned|P29|Early Permian|Late Carboniferous|Overlying unit is Purni Formation.||||||08-AUG-06
26505|Crown Point Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
26505|Crown Point Formation|24204|5|Briefly described|p262, 263 Fig.4, p266 Fig.7|Early Permian|Late Carboniferous|Geological Province: Pedirka Basin.||||||
26505|Crown Point Formation|29442|6|Mentioned|p103|||||||||
26505|Crown Point Formation|29591|6|Mentioned|p82|||||||||
26505|Crown Point Formation|30340|6|Mentioned|p2519|||Lithology||||||
26505|Crown Point Formation|30341|4|Described|p120|||Permian age. Pedirka Basin.||||||
26505|Crown Point Formation|30514|6|Mentioned|p100|||Permian age||||||
26505|Crown Point Formation|30544|5|Briefly described|p52|||See also Fig.6 p53.||||||08-AUG-06
26505|Crown Point Formation|30825|6|Mentioned|p37|||||||||
26505|Crown Point Formation|31567|6|Mentioned|p274|||Latest Carb.- early Permian. Unconformable on Finke Gp.||||||
26505|Crown Point Formation|32640|6|Mentioned|p241|||||||||
26505|Crown Point Formation|33103|6|Mentioned|p25|||||||||
26505|Crown Point Formation|33523|6|Mentioned|p23|||||||||
26505|Crown Point Formation|33824|6|Mentioned|p7|||||||||
26505|Crown Point Formation|33832|6|Mentioned|p7|||Stratigraphy||||||
26505|Crown Point Formation|33844|4|Described|p36|||||||||
26505|Crown Point Formation|33931|6|Mentioned|p9|||L.Perm.||||||
26505|Crown Point Formation|33971|3|Fully described|p32|||||||||
26505|Crown Point Formation|33976|6|Mentioned|p5|||||||||
26505|Crown Point Formation|34111|6|Mentioned|p16|||Permian||||||
26505|Crown Point Formation|34580|4|Described|Table 1|||Permian||||||
26505|Crown Point Formation|35845|6|Mentioned|Fig.25|||||||||
26505|Crown Point Formation|36473|6|Mentioned|Map legend|Permian|Permian|||||||
26505|Crown Point Formation|36733|6|Mentioned|p14|||||||||
26505|Crown Point Formation|36751|6|Mentioned|p489|||||||||
26505|Crown Point Formation|36899|6|Mentioned|p1089|||||||||
26505|Crown Point Formation|36922|6|Mentioned|p188|||||||||
26505|Crown Point Formation|37776|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|37855|6|Mentioned|p4|||See also Fig.2.||||||
26505|Crown Point Formation|37917|4|Described|p470|||||||||
26505|Crown Point Formation|39265|6|Mentioned|Fig. 3|||||||||
26505|Crown Point Formation|40637|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|40910|5|Briefly described|p15|||||||||
26505|Crown Point Formation|40911|6|Mentioned|Map legend|Permian|Carboniferous|||||||
26505|Crown Point Formation|40925|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
26505|Crown Point Formation|40926|3|Fully described|p12|||Mention Table 1||||||
26505|Crown Point Formation|41063|6|Mentioned|p46|||||||||
26505|Crown Point Formation|41183|6|Mentioned|Fig.3 p308|||||||||
26505|Crown Point Formation|41270|6|Mentioned|p279|||||||||
26505|Crown Point Formation|41491|6|Mentioned|Fig.8|||||||||
26505|Crown Point Formation|41689|6|Mentioned|Table 1|||||||||
26505|Crown Point Formation|42463|6|Mentioned|Fig.4 P171|||||||||
26505|Crown Point Formation|42504|5|Briefly described|p81|||||||||
26505|Crown Point Formation|42547|4|Described|p82|||||||||
26505|Crown Point Formation|42746|5|Briefly described|p3, Fig.2 p4|||Pedirka Basin||||||
26505|Crown Point Formation|42940|5|Briefly described|Plate 2|Permian|Permian|Sandstone, diamictite, shale, siltstone. Age: 290-250Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
26505|Crown Point Formation|43052|5|Briefly described|Table 2.1|||||||||
26505|Crown Point Formation|44133|5|Briefly described|p42, 65 Fig 8.4, 89|Permian|Carboniferous|Geological Province: Pedirka Basin. ||||||
26505|Crown Point Formation|44323|14|Not recorded|map legend||Permian|SG/53-6.||||||
26505|Crown Point Formation|44335|4|Described|p.11||Permian|Table 2. p.10||||||
26505|Crown Point Formation|44336|14|Not recorded|map legend||Permian|SG/53-3.||||||
26505|Crown Point Formation|44342|14|Not recorded|Not recorded|||||||||
26505|Crown Point Formation|44393|4|Described|p.6,8,Tb.1,Fig.1||Early Permian|L. Permian.||||||
26505|Crown Point Formation|44394|14|Not recorded|map legend||Early Permian|Lower Permian.||||||
26505|Crown Point Formation|45041|4|Described|p112|||Permian||||||
26505|Crown Point Formation|45104|6|Mentioned|p30|||||||||
26505|Crown Point Formation|45168|6|Mentioned|p10|||||||||
26505|Crown Point Formation|46849|6|Mentioned|p199|||||||||
26505|Crown Point Formation|48865|2|Defined|p.36||Permian|Fig.4. On many pages. p.21,28,33,34,37,39,41,48,51. Fig.13, Pl.6,11. (G53-6).||||||
26505|Crown Point Formation|48880|14|Not recorded|p.20||Permian|(map).||||||
26505|Crown Point Formation|48890|4|Described|p.53||Permian|||||||
26505|Crown Point Formation|48963|6|Mentioned|Plate 5|||||||||
26505|Crown Point Formation|62376|5|Briefly described|p84|Late Carboniferous|Late Carboniferous|Geological Province: Pedirka Basin.||||||09-FEB-10
26505|Crown Point Formation|64778|6|Mentioned|p13, 15-21, 23|Carboniferous|Carboniferous|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary. Potential hydrocarbon source rock.|314-285 Ma.|||||
26505|Crown Point Formation|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Late Carboniferous|Late Carboniferous|Geological province: Pedirka Basin. Periglacial deposits - dominantly a glacial succession, comprising diamictite, glacial-fluvial outwash, ripple laminated sandstone and siltstone, together with shale and varved successions. See also p8.||||||09-APR-13
26505|Crown Point Formation|65309|6|Mentioned|p21.|||Pedirka Basin. Useful as an aquifer.||||||
26505|Crown Point Formation|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 193 m.||||Overlies Idracowra Sandstone. Is overlain by De Souza Sandstone.||
26505|Crown Point Formation|65489|5|Briefly described|p55, p57-58, p60-61, p63-64, p137-139|Permian|Permian|See also p143, p151. Basal unit in the Pedirka Basin. Perhaps over 600m thick. Has reservoir potential.||||Is overlain by Purni Formation. Equivalent to Merrimelia Formation.|Fluvioglacial and glaciolacustrine sediments.|
26505|Crown Point Formation|67856|6|Mentioned|p348|||Of central Amadeus Basin.||||Correlated with Buck Formation and Ligertwood beds.||
26505|Crown Point Formation|69454|5|Briefly described|p38:1-6,7 Fig.38.6; 38:12-13,14 Fig.38.9|Asselian|Asselian|Wells et al. (1966). The only outcropping strata of the Pedirka Basin. Early Permian. 504m thick in Mount Hammersley-1. Crops out as mesas, buttes and low mounds. Glaciofluvial, glaciolacustrine and periglacial deposits. Sandstones have fair to good reservoir potential.||||Is overlain conformably by, and interfingers with, Tirrawarra Sandstone. Also overlain by Purni Formation. Correlated with Merrimelia, Boorthanna and Kuriyippi Formations.|Conglomerate, diamictite, cross-bedded pebbly and coarse sandstone, ripple-laminated fine sandstone and siltstone, thick claystone-dominated intervals with varvite bands.|12-JUL-16
26505|Crown Point Formation|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
26505|Crown Point Formation|69673|4|Described|p149, p150, p151, p160, p161 fig 131|Permian|Permian|Greater than 504m thick.||||Conformably overlain by Purni Formation,|Conglomerate, diamictite, cross bedded pebbly and coarse sandstone, ripple laminated fine sandstone and siltstone.|
26505|Crown Point Formation|69946|4|Described|p5-6, p36, p44-48, p51|Asselian|Late Carboniferous|Pedirka Basin. Defined by Wells et al. (1966) to replace the informal Crown Point Series. Type section is at One Tree Point, near Crown Point, NT. Diamictite clasts are derived from early Paleozoic sediments and Musgrave Province. Up to 347m thick.||||Is overlain disconformably by Purni Formation or Stuart Range Formation equivalent. Correlates with Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine- to coarse-grained sandstone with interbeds of medium to dark grey siltstone and diamictite units containing faceted and striated exotic pebbles and cobbles.|
26505|Crown Point Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Is overlain conformably by Stuart Range Formation and (locally) unconformably by Purni Formation.||
26505|Crown Point Formation|71342|4|Described|Ch4 p25, Ch5 p5-p6|Early Permian|Late Carboniferous|Pedirka Basin. Formally defined by Wells et al (1966) to replace the informal Crown Point Series. A type section outcropping at One Tree Point on the FINKE 1:250000 map area in the NT is mentioned. Lithology discussed in further detail. This unit has a maximum thickness of 347m at Mount Hammersley 1. Sedimentology is briefly described. Deposited in periglacial, interglacial, fluvioglacial or glaciolacustrine environments. See also Ch5 p30, Ch5 p36, Ch5 p44-p48, Ch5 p51, Ch8 p28, Ch9 p9, Ch9 p11, Ch9 p16, Ch9 p18, Ch9 p20-p21, Ch11 p6-p7, Ch11 p18, Ch12 p7.||||Unconformably overlies the Finke Group. Disconformably overlain by the Purni Formation. Equivalent to the Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine to coarse-grained sandstone with interbeds of medium to dark grey siltstone.|
26505|Crown Point Formation|72476|6|Mentioned|p26, p36 Fig.9|Permian|Carboniferous|Perdika Basin. Time-temperature thermal history diagram.||||||
26505|Crown Point Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Pedirka Basin. See DIP034_Petroleumdata.xlsx.||||||
80769|Crusader Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.||Argylla Formation, Magna Lynn Metabasalt|||Quartzose to lithofeldspathic sandstone and pebble to cobble conglomerate containing clasts of quartz, quartzite, felsic and minor mafic volcanics.|
81906|Crush Creek Coal Measures|73029|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Very fine to coarse-grained, thin to medium-bedded sandstone, locally flaggy, volcaniclastic sandstone, and quartz pebble to cobble conglomerate; local thin basalt flows; some carbonaceous siltstone and rare coal.|
36104|Crystal Brook Volcanic Neck|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Units Cgg, Ootann Supersuite and units Cgb, Cgm, Almaden Supersuite.||||||
39145|Crystal Vale Monzogranite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Leucocratic biotite granite.||||||
39145|Crystal Vale Monzogranite|65388|3|Fully described|p246-247, p236 Fig. 81|Carboniferous|Carboniferous|Previously Crystal Vale Adamellite.  Interpreted by Whitaker & others (1974), to intrude Moocoorooba Granite and Glencoe Gabbro, but foliation, gneiss and recrystallisation now suggests that the Glencoe Gabbro intruded Crystal Vale Monzogranite. Intruded by Cretaceous Mount Runsome Basalt. Two K-Ar ages: Green (1975) and Whitaker & others (1974), originally interpreted to belong to the "Glandore Granodiorite" are now considered to be from Crystal Vale Monzogranite.  Biotite age: 246Ma, hornblende age: 319Ma. Monzogranite in east, hornblende gabbro, diorite, granodiorite and tonalite in west.||||||
39145|Crystal Vale Monzogranite|68679|5|Briefly described|p407, p419|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Two small, irregular areas: assignment of western area to this unit is very uncertain. K-Ar (biotite) and K-Ar (hornblende) ages respectively, both in the western area, by Whitaker et al. (1974).|319 +/- 9 Ma and 246 +/- 5 Ma.|||May be intruded by Glencoe Gabbro.|Eastern outcrop: medium- to coarse-grained hornblende-biotite monzogranite and pink muscovite leucogranite; some coarse-grained biotite gneiss. Western outcrop: hornblende gabbro, diorite, tonalite and medium-grained melanocratic granodiorite.|
83539|Cudgee Creek Granite|73527|5|Briefly described|p2, p8-9, p14|Calymmian|Calymmian|Classified as a hybrid granite between I- and A-type. Located between the Georgetown and Mount Isa Inliers. Abbreviated as Cudgee p4 Fig.3, p6. Sampled in drill cores drill cores HB1 347 and HB2 315.|ca. 1545 Ma (Nordsvan, 2020)||||Megacrystic granite containing hornblende, titanite and allanite.|
83539|Cudgee Creek Granite|73642|5|Briefly described|p4, p5 Tb.2, p6, p8 Fig.6, p9, p11-13|Calymmian|Calymmian|Newly identified. I-/A-type granite. eHf values of 0 to +4. Also shown as Cudgee Creek granite. See also Cudgee Creek Granites p5 Fig.3, p10 Fig.8, p11-13.|1544+/-6 Ma, 1545+/-8 Ma||||Granites|
24233|Culba Granodiorite|22669|6|Mentioned|P259||Visean|||||||
24233|Culba Granodiorite|23032|4|Described|p43|||||||||
24233|Culba Granodiorite|23291|4|Described|p50, p98 Tb. 3.11|Carboniferous|Carboniferous|Age: 335Ma (Rb-Sr). Geological Province: Georgetown Region.||||||18-JUN-15
24233|Culba Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No.34. I-Type.||||||
24233|Culba Granodiorite|35920|2|Defined|p25|Carboniferous|Carboniferous|Prob. Carboniferous||||||
24233|Culba Granodiorite|36937|6|Mentioned|p229|||||||||
24233|Culba Granodiorite|37576|5|Briefly described|p8|||||||||
24233|Culba Granodiorite|39445|6|Mentioned|p72|||See also P148||||||
24233|Culba Granodiorite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24233|Culba Granodiorite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
24233|Culba Granodiorite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
24233|Culba Granodiorite|43664|6|Mentioned|p96|||||||||
24233|Culba Granodiorite|43740|4|Described|p26||Carboniferous|||||||
24233|Culba Granodiorite|50200|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||
24233|Culba Granodiorite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||14-MAY-04
24233|Culba Granodiorite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Bagstowe Ring Structure, Kennedy Province. Strongly magnetic.|||||Grey hornblende-biotite granodiorite; greyish-pink, fine- to medium-grained biotite granite.|
24233|Culba Granodiorite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Grey hornblende-biotite granodiorite.|
24233|Culba Granodiorite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Biotite to hornblende-biotite granodiorite. I-type.|
28043|Culpin Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes the Holroyd Group||||||
28043|Culpin Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p35|||Of Ebagoola Suite (Kintore Supersuite). Intrudes Carysfort and Sugarbag Creek Quartzites, Astrea and Dinah Fms., and Yellowood granodiorite. pale grey to buff, equgranular muscovite-biotite granite; weakly foliated in places.||||||27-JAN-09
28043|Culpin Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
24894|Cumberland Range Volcanic Group|23291|4|Described|p42,48, p91 Tb. 3.8|||Originally named Cumberland Range Volcanics. Geological Province: Georgetown Region.||||||18-MAY-15
24894|Cumberland Range Volcanic Group|23430|6|Mentioned|p499|||||||||
24894|Cumberland Range Volcanic Group|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24894|Cumberland Range Volcanic Group|40860|6|Mentioned|Fig.1|||||||||
24894|Cumberland Range Volcanic Group|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
24894|Cumberland Range Volcanic Group|43740|4|Described|p21|||||||||
24894|Cumberland Range Volcanic Group|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Includes: Scrubby Creek Rhyolite, Dismal Creek Dacite, Marquis Rhyolite, Namul Dacite.||||||
24894|Cumberland Range Volcanic Group|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron.|||Includes Scrubby Creek and Marquis Rhyolites; Namul and Dismal Creek Dacites.|||
24894|Cumberland Range Volcanic Group|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
24894|Cumberland Range Volcanic Group|69591|6|Mentioned|p102|Carboniferous|Carboniferous|||||Overlies Gilberton Formation.||
24894|Cumberland Range Volcanic Group|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association.|||||Biotite granite and microgranite to rhyolite; hornblende-biotite and biotite microgranodiorite to microtonalite. I-type.|
24894|Cumberland Range Volcanic Group|72983|6|Mentioned|p78|||||||Intruded by and is possibly co-magmatic with Mount Darcy microgranodiorite.||
79947|Cumbooromon Bore Granite|71251|6|Mentioned|p3|||Yowah-Cunnamulla area.||||||
79947|Cumbooromon Bore Granite|71864|6|Mentioned|p3|||||||||
25868|Curalle silcrete profile|35793|2|Defined|p248|Miocene|Oligocene|Oligocene to Miocene||||||
25868|Curalle silcrete profile|61007|5|Briefly described|p296|||May have formed at the same time as the Morney and Canaway silcrete profiles - in quartzose sediments in lowlands. In the Clarence-Moreton Basin area.||||||
25868|Curalle silcrete profile|61155|6|Mentioned|p17|Early Oligocene|Early Oligocene|Informal name. In southwest Queensland. ||||||
24237|Curlew Formation|24420|5|Briefly described|p9|Eocene|Eocene|Of The Narrows Group.||||||
24237|Curlew Formation|24490|5|Briefly described|Map Legend|Tertiary|Tertiary|Claystone, carbonaceous shale, sandstone, limestone. In the Narrows Graben.||||||04-SEP-08
24237|Curlew Formation|37628|6|Mentioned|p196|||||||||
24237|Curlew Formation|37676|4|Described|p11|||||||||
24237|Curlew Formation|38658|6|Mentioned|p152|||||||||
24237|Curlew Formation|39445|6|Mentioned|p169|||||||||
24237|Curlew Formation|39493|6|Mentioned|p94|||||||||
24237|Curlew Formation|40116|4|Described|p39|||||||||
24237|Curlew Formation|41927|4|Described|p68|||||||||
24237|Curlew Formation|42021|5|Briefly described|p321|||||||||
24237|Curlew Formation|42340|5|Briefly described|p25||middle Eocene|||||||
24237|Curlew Formation|50207|5|Briefly described|Map Legend|Tertiary|Tertiary|Of the The Narrows Group.||||||
24237|Curlew Formation|68008|4|Described|p271|Eocene|Eocene|Henstridge and Missen (1982), who subdivided The Narrows Beds of Kirkegaard et al. (1970). The type section is a composite section, based on core from two boreholes: GSQ Rockhampton 2 and Southern Pacific Petroleum's RD66. Occurs mainly in the N part of the Graben.||Upper The Narrows Group.||Overlies the Rundle Formation.|Mudstone, carbonaceous siltstone, and minor calcareous sandstone and limestone.|
24237|Curlew Formation|71092|5|Briefly described|p232-233|Eocene|Eocene|The Narrows Graben, SE Queensland. Middle-late Eocene age from fossil flora.||||Overlies Rundle Formation.||
24237|Curlew Formation|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||||Overlies Kerosene Creek Member (Rundle Formation).||
41167|Curraghmore Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
41167|Curraghmore Granite|60425|4|Described|p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla Supersuite). S-type. Composite unit of 2 muscovite-garnet-biotite granite subunits, one of which is locally gneissic and foliated, and the other is deformed and intrudes the first - detailed lithology included.||||||07-FEB-11
41167|Curraghmore Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Curraghmore Suite.||||
69325|Curraghmore Suite|60425|5|Briefly described|p81 Tb. 5|||Of the Whypalla Supersuite. S-type.||||||07-FEB-11
69325|Curraghmore Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Curraghmore, Desailly, Kelly Saint George, McLeod, Nangeee, Northedge Granites.|||
77833|Currawinya Granite|68553|6|Mentioned|Map legend|Late Devonian|Middle Devonian|This unit and the Eulo Granite are mapped under the same symbol, Dge.||||||
77833|Currawinya Granite|68731|5|Briefly described|p166, p167 Tb 3.2|Late Devonian|Middle Devonian|I-type granite. Detailed lithology discussed on p167. See also Eulo Ridge Granite.|381.5 +/- 2.4 Ma||||Pale pink to pale pinkish grey, fine- to coarse-grained (mainly medium-grained), highly porphyritic biotite monzogranite; pale pink K-feldspar phenocrysts to ~ 5cm; feldspar phenocrysts aligned; deformed and partly recrystallised.|10-MAY-16
77833|Currawinya Granite|68823|5|Briefly described|p393|Givetian|Givetian|Geochronology by Bultitude and Cross (2012).|381.3 +/- 2.42 Ma, SHRIMP-IIe|||||
77833|Currawinya Granite|68901|5|Briefly described|p7|Late Devonian|Middle Devonian|Eulo Ridge, Thomson Region.|||||Pink, porphyritic bioitite monzogranite.|26-SEP-18
77833|Currawinya Granite|69952|5|Briefly described|p1, p2 Tb.i, p16, p34-37|Late Devonian|Late Devonian|Southern part of the Eulo Ridge, Thomson Orogen. SHRIMP U-Pb zircon age of emplacement.|381.5 +/- 2.5 Ma (Cross et al., 2015).||||Pink, porphyritic biotite granite.|
77833|Currawinya Granite|70720|5|Briefly described|p2, p8|Devonian|Devonian|Eulo Ridge, southern Thomson Orogen. Roughly tabular-shaped domains with irregular magnetic high trends.|381.5 +/- 2.4 Ma (SHRIMP U-Pb zircon).||||Foliated, coarse-grained biotite granite.|
77833|Currawinya Granite|70821|5|Briefly described|p9-10, p13 Tb.2.1|Late Devonian|Middle Devonian||381.5 +/- 2.4 Ma (Bultitude and Cross, 2013).||||Includes monzogranite.|01-DEC-16
77833|Currawinya Granite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|382+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
77833|Currawinya Granite|71965|5|Briefly described|p897,901,906,913-914|||Geological province: Thomson Orogen. Outcropping I-type granite in the southern Thomson Orogen.|381.5+\-2.5 Ma|||Correlable with Waihora Volcanics.|Weakly foliated, pink, porphyritic medium- to coarse-grained biotite rapakivi monzogranite.|
77833|Currawinya Granite|71966|5|Briefly described|p988-995,998-999,1001-1002,1004-1005|Late Devonian|Late Devonian|Geological province: southern Thomson Orogen. I-type granite. Reflects a period of Middle Devonian c. 395-380 Ma magmatism. Sample 2122056 yielded an age of 381.5+\-2.5 Ma, which is interpreted as the crystallisation age of this rock. Hf and O isotopic anaylsis indicate uncommon patterns of of near-juvenile to juvenile EHF values, but supracrustal O isotope signatures, which may be explained by reworking of juvenile sediments sourced from nearby, Early Devonian juvenile magmatism, related to contraction during the Tabberabberan Orogeny.|381.5+\-2.4 Ma|||||
77833|Currawinya Granite|72522|5|Briefly described|p49|Late Devonian|Middle Devonian|Along Eulo Ridge, south of Granite Springs Granite.|381.3+/-2.5 Ma|||||
77833|Currawinya Granite|73179|6|Mentioned|p1152|Frasnian|Givetian|Thomson Orogen, southern. Geochron from Cross et al. (2015).|381.5 +/- 2.5 Ma|||||
38868|Cynthia beds|24488|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38868|Cynthia beds|24615|5|Briefly described|CD|Middle Triassic|Middle Triassic|[Rvy].  Boulder conglomerate, lithic sandstone, rhyolitic and andesitic volcanics, siltstone, shale.||||||
38868|Cynthia beds|64398|5|Briefly described|Map legend|Late Triassic|Middle Triassic|Age: Middle Triassic? - Late Triassic? Boulder conglomerate, lithic sandstone, rhyolitic and andesitic volcanics, siltstone, shale.||||||14-AUG-08
38868|Cynthia beds|64399|5|Briefly described|Map legend|Triassic|Triassic|Unconformably overlie Nogo beds; unerlie Precipice Sandstone. Boulder conglomerate, lithic sandstone, rhyolitic to andesitic volcanics, siltstone, shale.||||||19-AUG-08
38868|Cynthia beds|65388|6|Mentioned|p209|Middle Triassic|Middle Triassic|Abercorn Trough. Unconformably overlain by Precipice Sandstone.||||||
38868|Cynthia beds|67402|5|Briefly described|p204, p209, p239|Ladinian|Anisian|Abercorn Trough. Unsuitable for the storage of carbon dioxide. ||||Overlies the Cabawin Formation.|Fresh water boulder conglomerate, lithic labile sandstone, rhyolitic and andesitic volcanics, siltstone and shale.|
38868|Cynthia beds|68008|4|Described|p186-188, p195, p492|Middle Triassic|Middle Triassic|Whitaker et al. (1974). Previously described by Dear et al. (1971) as part of Muncon Volcanics. Abercorn Trough, Mulgildie Basin. Forms two SSE-trending fault blocks 16 x 2 km. From 180m to 1500m thick. Has moderate to steep dips to the W.||||Faulted against Rockhampton Group and Youlambie Conglomerate, and Hutton Sandstone and Mulgildie Coal Measures (also unconformably underlies the last two). Correlated with Toogoolawah Group.|Khaki-coloured conglomerate grading into feldspathic sandstone, thick beds of agglomerate and lapilli tuff; interbedded are volcaniclastic sandstone and mudstone and minor andesitic flows.|
38868|Cynthia beds|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
38868|Cynthia beds|68679|5|Briefly described|p312-313, p388, p397-398|Middle Triassic|Early Triassic|Whitaker et al. (1974). Fills the Abercorn Trough, Northern New England Orogen. Crops out poorly; better known from petroleum exploration wells. Fluvial to lacustrine environments. Some petroleum source rock potential, but reservoir potential is very poor.||||Probably equivalent to Moolayember and Esk Formations and Clematis Group.|Mainly poorly sorted, quartz-poor, clast-supported conglomerate and volcaniclastic sandstone. Drill hole reports suggest finer sediments dominate: interbedded sandstone, siltstone, shale, mudstone and volcanics with minor conglomerate and coal.|
33148|Dacey Granite|23042|5|Briefly described|p19,74,5, Fig 2||Late Carboniferous|||||||
33148|Dacey Granite|60475|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|White to pink, medium grained, biotite-hornblende granite with hornblende cyrstals ranging up to 1.5cm.||||||
33148|Dacey Granite|61035|4|Described|p7, p9 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Mount Whelan + Mountain View Volcanics. Age: 316+/-2.3Ma (M. Fanning, SHRIMP). Geological Province: Connors Sudprovince. Medium-grained, biotite-hornblende granite.||||||07-FEB-11
33148|Dacey Granite|65388|2|Defined|p356, p90 Fig. 37, p94, 98, 394, 399|Late Carboniferous|Late Carboniferous|Connors Arch pluton.  Intrudes Mountain View Volcanics, Whelan Creek Volcanics. Co-magmaitc with Whelan Creek Volcanics? Ages within error. SHRIMP dating gave an age of 316.5+/- 4.1Ma (MSWD = 1.9 on 18 grains). Medium grained white to pink, biotite-hornblende granite or granodiorite in type section. Elsewhere typically altered and weathered commonly intruded by felsic to intermediate dykes.||||||
33148|Dacey Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Olympus,Toobier, Tooloombah Creek and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
33148|Dacey Granite|68679|5|Briefly described|p347, p353, p356, p362|Carboniferous|Carboniferous|Southern Connors Subprovince, northern New England Orogen.|313.0 +/- 4.0 Ma (SHRIMP: Fanning et al., 2009).|||Intrudes Whelan Creek Volcanics (Connors Volcanic Group).||
33148|Dacey Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|313+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
23527|Dagworth Andesite|23291|4|Described|p95 Tb. 3.10|Early Permian|Early Permian|Parent: Namarrong Volcanic Subgroup. Age: 283+/-3Ma. Thickness: Up to 380m. Geological Province: Georgetown Region.||||||28-MAY-15
23527|Dagworth Andesite|23510|5|Briefly described|Map Legend||Early Permian|of Namarrong Volcanic Subgroup, Newcastle Range Volcanic Group.||||||
23527|Dagworth Andesite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V15.||||||
23527|Dagworth Andesite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23527|Dagworth Andesite|40542|6|Mentioned|p97|||||||||
23527|Dagworth Andesite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Namarrong Volcanic Subgroup.||||||
23527|Dagworth Andesite|43740|4|Described|p10|||||||||
23527|Dagworth Andesite|50198|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Nammarong Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
23527|Dagworth Andesite|68354|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Age min: Early Permian?||Unit in Nammarong Volcanic Subgroup. [misspelling of Namarrong Volcanic Subgroup]|||Grey to green and purple aphyric to abundantly porphyritic augite-pigeonite basaltic andesite.|08-JUL-15
73614|Dahls Hill Complex|65452|6|Mentioned|p6 Fig.2|||||||||
73614|Dahls Hill Complex|67203|5|Briefly described|p6, p9-10 Fig.5, p31|Permian|Late Carboniferous|West and southwest Bobby Range area.|||||Higher-grade metasediments, locally interleaved with granitic/pegmatitic material; foliated medium- to coarse-grained biotite monzogranite.|
73614|Dahls Hill Complex|68319|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Wandilla Province. Minimum age is Early Permian.|||||Dark grey, fine to medium-grained, nebulitic biotite and biotite-muscovite orthogneiss, migmatite, interleaved granite rocks and minor muscovite schist.|
73614|Dahls Hill Complex|68421|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Coastal Subprovince, Wandilla Province. U-Pb zircon ages (Carson et al. 2006).|320 Ma (detrital), 282.4 +/- 2.5 Ma (metamorphic)|||Intrudes the Gaythorn Metamorphics and Duckpond Road Metamorphics.|Dark grey, medium-grained, nebulitic biotite and biotite-muscovite orthogneiss, migmatite, interleaved granitic rocks and minor muscovite schist.|
36626|Dalbeg granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 480.  I-Type.||||||
23529|Dalkum Microgranite|23420|5|Briefly described|p 147 table 4.6|Permian|Late Carboniferous|In the Ootann Supersuite of the Cape York Penninsula Batholith||||||
23529|Dalkum Microgranite|42772|6|Mentioned|Fig.18|||||||||
23529|Dalkum Microgranite|43083|6|Mentioned|p109 Tb. 7, p125|||May form part of the O'Briens Creek Supersuite? But Table 7 states it is not assigned to any suite/supersuite.||||||17-JUN-09
23529|Dalkum Microgranite|60357|5|Briefly described|Map Legend|Permian|Late Carboniferous|Geological Province: Kennedy Province. Biotite leucogranite.||||||
74882|Dalma Basalt|68008|2|Defined|p225, p233, p243, p246, p248, p250-255|Early Cretaceous|Early Cretaceous|See also p261, p264, p266-267, p269, p393, p493, p530, p565. New name, for Early Cretaceous basalts in the Mount Morgan-Westwood-Stanwell-Dalma area that overlie Precipice Sandstone; distinct from Late Cretaceous Alton Downs Basalt. All of these had been mapped and regarded as Late Cretaceous by Kirkegaard et al. (1970). Named for the Dalma district 17km NNW of Stanwell: three main outcrops described. The type section is along the Stanwell-Daroula road, from 13km NW of Stanwell to the (abandoned) Dalma school. Forms low plateaux, undulating hills and terraces; weathers to brown soil. Unconformably overlies Mount Alma and Lorray Formations, Rockhampton Group, Dinner Creek Conglomerate, Native Cat Andesite, Bushley Dacite, Ridgelands Granodiorite, Wycarbah Volcanics (?locally conformably)and Precipice Sandstone. Geochemistry detailed; compared with Alton Downs Basalt: may be the same unit. Repeatedly refers to Dalma Basalt as "forming the base of the Mount Salmon Volcanics", but the authors do not define it as a Member. Between 67m and 180m thick. Rb-Sr data tabulated.|c.120 Ma or c.113 Ma (Rb-Sr isochron).|||Is overlain by Stanwell Formation (possibly conformably) and Mount Salmon Volcanics conformably.|Dark grey, fine-grained basalt, sparsely porphyritic in plagioclase and olivine.|
74882|Dalma Basalt|69594|5|Briefly described|p551-552, p559-560, p563, p565|Early Cretaceous|Early Cretaceous|Stanwell Basin. Occurs E of Mount Salmon, around Dalma, and W and SW of Wycarbah. Previously mapped as Late Cretaceous. >67m thick. Appears identical to the Alton Downs Basalt.||||Overlies Wycarbah Volcanics and Precipice Sandstone. Is overlain conformably by Mount Salmon Volcanics and Stanwell Formation. May be part-equivalent to the Alton Downs Basalt.|Dark grey, relatively uniform, fine-grained, sparsely porphyritic plagioclase- and olivine-phyric basaltic lavas.|
74882|Dalma Basalt|73450|5|Briefly described|p51-54|Cretaceous|Cretaceous|Probably part of the same episode of within-plate volcanism as the Wycarbah Volcanics. Considered the base of the sequence that includes the Mount Salmon Volcanics.||||Underlain by Wycarbah Volcanics. Conformably overlain by Mount Salmon Volcanics.||
29262|Dalmore Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
29262|Dalmore Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
29262|Dalmore Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
29262|Dalmore Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 121. I-Type||||||
29262|Dalmore Granodiorite|42245|2|Defined|p40|Early Devonian|Late Silurian|||||||
29262|Dalmore Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
29262|Dalmore Granodiorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Late Silurian-Early Devonian?||||||
29262|Dalmore Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
29262|Dalmore Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
29262|Dalmore Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Dalmore gdrt.||Unit in Millchester Supersuite.||||
33424|Dangore Volcanics|23799|3|Fully described|p109, p11 Tb. 1|Late Triassic|Late Triassic|Previously mapped as part of Main Range Volcanics.  Max. thickness: ~200m.  Geological Province: Yarraman Subprovince.  See also p127.||||||
33424|Dangore Volcanics|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
33424|Dangore Volcanics|60371|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Massive, cream rhyolitic ignimbrite; minor siltstone, shale.||||||
33424|Dangore Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
33424|Dangore Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
33424|Dangore Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
33424|Dangore Volcanics|68679|5|Briefly described|p312-313, p413, p434, p441|Late Triassic|Late Triassic|West of Gayndah, northern New England Orogen. Age from correlation with Aranbanga Volcanic Group.||||Overlies Boondooma Igneous Complex. Is correlated with Aranbanga Volcanic Group.|Rhyolite breccia with angular granule- to cobble-sized flow-banded rhyolite clasts in an ashy groundmass, and a crystal-rich to crystal- and lithic-rich rhyolitic ignimbrite.|
26300|Daniel Creek Formation|22533|6|Mentioned|p55|||In Georgetown Region||||||
26300|Daniel Creek Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Glen Ido Schist and lower sequence of the Willyama Supergroup.||||||07-NOV-08
26300|Daniel Creek Formation|23032|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26300|Daniel Creek Formation|23220|5|Briefly described|Fig.2 p9|||Of Robertson River Subgroup.||||||15-JAN-07
26300|Daniel Creek Formation|23291|4|Described|p86 Tab. 3.6, p23|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Group. Overlain by Dead Horse Metabasalt; underlain by Bernecker Creek Formation. Geological Province: Georgetown Region.||||||08-JUL-15
26300|Daniel Creek Formation|23431|5|Briefly described|p530|||Possibly laterally equivalent to Einasleigh Metamorphics.  Of Etheridge Group||||||
26300|Daniel Creek Formation|38714|2|Defined|p186|Mesoproterozoic|Mesoproterozoic|||||||
26300|Daniel Creek Formation|38715|6|Mentioned|p191|||||||||
26300|Daniel Creek Formation|39495|6|Mentioned|p142|||||||||
26300|Daniel Creek Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
26300|Daniel Creek Formation|39924|6|Mentioned|p341|||||||||
26300|Daniel Creek Formation|41272|5|Briefly described|M 1of1 H06|||See also M 1of1 J04||||||
26300|Daniel Creek Formation|41675|6|Mentioned|p7|||||||||
26300|Daniel Creek Formation|41680|6|Mentioned|p107|||||||||
26300|Daniel Creek Formation|41975|4|Described|p436|||||||||
26300|Daniel Creek Formation|42199|5|Briefly described|Table 1 P280|||||||||
26300|Daniel Creek Formation|43060|5|Briefly described|p28|||Of Robertson River Subgroup.||||||15-JAN-07
26300|Daniel Creek Formation|43480|6|Mentioned|10-47|||||||||
26300|Daniel Creek Formation|43664|4|Described|p23-25|||||||||
26300|Daniel Creek Formation|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
26300|Daniel Creek Formation|50199|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group). Includes the Mount Helpman Member.||||||18-JUN-15
26300|Daniel Creek Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup.  Underlies: Dead Horse Metabasalt.  Intruded by Cobbold Metadolerite.||||||19-JUN-13
26300|Daniel Creek Formation|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group). Overlies Bernecker Creek Formation. Conformably overlain by Dead Horse Metabasalt. Intruded by Cobbold Metadolerite.||||||07-NOV-08
26300|Daniel Creek Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||30-JUL-04
26300|Daniel Creek Formation|50595|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Underlies: Corbett Formation.||||||07-NOV-08
26300|Daniel Creek Formation|61258|5|Briefly described|p386, p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Lower part of the Robertson River Subgroup (Etheridge Group). Overlies the Bernecker Creek Formation. Geological Province: Georgetown Inlier.||||||07-NOV-08
26300|Daniel Creek Formation|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
26300|Daniel Creek Formation|65887|5|Briefly described|p41, p47|Statherian|Paleoproterozoic|Of Robertson River Subgroup. Overlain by Dead Horse Metabasalt.||||||
26300|Daniel Creek Formation|66800|5|Briefly described|p925, p928, pp932-933.|Proterozoic|Proterozoic|Western subdivision of Etheridge Group. Suggested correlation with Einasleigh Metamorphics.|Probably 1674.9 +/- 3.3 Ma.|Unit in Robertson River Subgroup.||Overlies Bernecker Creek Formation. Is overlain by Dead Horse Metabasalt.|Slightly calcareous and/or dolomitic, more pelitic, mudstone, siltstone and fine-grained sandstone.|
26300|Daniel Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Georgetown-Coen-Yambo Inliers.|Protoliths deposited ~1720-1690 Ma.|Lower Etheridge Group.||||
26300|Daniel Creek Formation|67341|5|Briefly described|vi, p5-9|||Forsayth Subprovince, Etheridge Province. Maximum depositional age.|1695 +/- 13 Ma (SHRIMP U-Pb zircon).|||Overlies Bernecker Creek Formation. Is overlain by Dead Horse Metabasalt.|Includes grey, fine-grained sandstone interbedded with thinly-bedded siltstones.|
26300|Daniel Creek Formation|67430|6|Mentioned|p25|||||||||
26300|Daniel Creek Formation|68352|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Is intruded by Cobbold Metadolerite. Is overlain conformably by Corbett Formation.|Mica schist, quartzite and some calc-silicate rocks.|
26300|Daniel Creek Formation|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1670 Ma.|Unit in Robertson River Subgroup.|Includes Mount Helpman Member.|Conformably overlies Bernecker Creek Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Dead Horse Metabasalt.|Mica schist, quartzite and some calc-silicate rocks; abundant muscovite granite and pegmatite dykes and small stocks.|
26300|Daniel Creek Formation|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1670 Ma.|Unit in Robertson River Subgroup.||Is intruded by Cobbold Metadolerite.|Mica schist, quartzite and some calc-silicate rocks.|
26300|Daniel Creek Formation|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Weakly to non-magnetic.|c.1670 Ma.|Unit in Robertson River Subgroup.||Conformably overlies Bernecker Creek Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Dead Horse Metabasalt.|Mica schist, quartzite and some calc-silicate rocks; grades into mudstone, siltstone and fine subfeldspathic sandstone, locally calcareous and/or dolomitic.|
26300|Daniel Creek Formation|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Of the Robertson River Subgroup.||Intruded by the Cobbold Metadolerite. Is overlain conformably by Dead Horse Metabasalt.|Mudstone, siltstone and fine subfeldspathic sandstone, locally calcareous and/or dolomitic.|
26300|Daniel Creek Formation|68576|6|Mentioned|Q_11: p24|||Georgetown area.||||||
26300|Daniel Creek Formation|69582|6|Mentioned|p76|||Etheridge Province. Intersected in GSQ Georgetown 8-9R.||Robertson River Subgroup||||
26300|Daniel Creek Formation|69591|4|Described|p61-62, p64, p68, p107|Paleoproterozoic|Paleoproterozoic|Forsayth Subprovince, Etheridge Province. 1000-2000m thick. Intense deformation has transposed bedding parallel to the foliation. Detrital zircon spectra.|~1695 Ma.|Robertson River Subgroup.||Overlies Bernecker Creek Formation.|Fine, subfeldspathic sandstone, siltstone and mudstone; grades into mica schist and quartzite which preserve only gross sedimentary features (eg bedding and laminations).|
26300|Daniel Creek Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1700 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
26300|Daniel Creek Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Georgetown area.|ca 1700 Ma|||Overlies the Bemecker Creek Formation. Overlain by the Dead Horse Metabasalt.|Sandstone and greywacke.|
26300|Daniel Creek Formation|73387|5|Briefly described|p9, p15, p18|Paleoproterozoic|Paleoproterozoic|Intruded by rhyolite dykes at the historic Homeward Bound gold mine.||Etheridge Group|||Includes micaceous siltstone, quartzite, and localised calc-silicate rocks.|20-DEC-22
27758|Dargalong Metamorphics|22781|6|Mentioned|p11|||||||||
27758|Dargalong Metamorphics|23076|5|Briefly described|p723||Proterozoic|||||||
27758|Dargalong Metamorphics|23220|6|Mentioned|Fig.1|||of Forsayth Subprovince.||||||
27758|Dargalong Metamorphics|23420|5|Briefly described|p 118|||||||||
27758|Dargalong Metamorphics|23422|5|Briefly described|Plate 7.3|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|23430|5|Briefly described|p451|||||||||
27758|Dargalong Metamorphics|23496|5|Briefly described|p47||Proterozoic|Underlies Pratt Volcanics.||||||
27758|Dargalong Metamorphics|23498|6|Mentioned|p25 table 1|||||||||
27758|Dargalong Metamorphics|23500|5|Briefly described|Map legend||Paleoproterozoic|Age: Palaeoproterozoic - Mesoproterozoic?||||||07-NOV-08
27758|Dargalong Metamorphics|23501|5|Briefly described|map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27758|Dargalong Metamorphics|23616|5|Briefly described|p5, Table 1C p17 p7||Proterozoic|Age: Proterozoic; probably >1650 Ma. Transitional relationship with lower grade McDevitt Metamorphics; intruded by various aged granitoids; faulted against Palaeozoic Hodgkinson Basin. Dargalong Inlier.||||||
27758|Dargalong Metamorphics|23624|6|Mentioned|p5|||||||||
27758|Dargalong Metamorphics|23713|3|Fully described|p8 Table 1||Mesoproterozoic|Intruded by the Nundah Granodiorite.  Overlying Unit Pratt Volcanics - unconformable and Gilbert River Formation - unconformable.||||||
27758|Dargalong Metamorphics|24080|5|Briefly described|p445 Fig. 4|Precambrian|Precambrian|Schist, gneiss and quartzite.  Geological Province: Laura Basin.||||||
27758|Dargalong Metamorphics|24485|3|Fully described|p8 Tb.1, p21, 22|Mesoproterozoic|Mesoproterozoic|Age: ~1640-1580Ma. Extensively intruded by the Nundah Granodiorite. Correlated with the Einasleigh Metamorphics. Geological Province: Yambo Subprovince.||||||03-JUN-09
27758|Dargalong Metamorphics|24486|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Yambo Sub-province (Etheridge Province).||||||07-NOV-08
27758|Dargalong Metamorphics|24487|5|Briefly described|Map legend|||||||||
27758|Dargalong Metamorphics|30257|5|Briefly described|p286|||See also P297 for dating.||||||
27758|Dargalong Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|31168|4|Described|p8|||||||||
27758|Dargalong Metamorphics|31453|6|Mentioned|p617|||||||||
27758|Dargalong Metamorphics|31812|4|Described|p481|||Pre-Cambrian. Refers de Keyser & Wolff (1964)||||||
27758|Dargalong Metamorphics|31822|6|Mentioned|p69|||Precambrian||||||
27758|Dargalong Metamorphics|31832|6|Mentioned|Table 6|||||||||
27758|Dargalong Metamorphics|32528|5|Briefly described|Table 1|||||||||
27758|Dargalong Metamorphics|32633|5|Briefly described|p439|||||||||
27758|Dargalong Metamorphics|32634|6|Mentioned|p29|||Proterozoic||||||
27758|Dargalong Metamorphics|33179|4|Described|Table 1|||||||||
27758|Dargalong Metamorphics|33180|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|33528|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|33635|5|Briefly described|p758|||||||||
27758|Dargalong Metamorphics|34581|4|Described|p132|||See also PP130,131,134 etc. Precambrian||||||
27758|Dargalong Metamorphics|34955|6|Mentioned|p228|||||||||
27758|Dargalong Metamorphics|35204|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|35220|4|Described|Table 1|||||||||
27758|Dargalong Metamorphics|35429|6|Mentioned|p126|||||||||
27758|Dargalong Metamorphics|36101|6|Mentioned|p167|||||||||
27758|Dargalong Metamorphics|37570|4|Described|p122|||||||||
27758|Dargalong Metamorphics|37609|6|Mentioned|p307|||||||||
27758|Dargalong Metamorphics|39445|5|Briefly described|p44|||Correlated with rocks in Yambo Inlier. See also Table 2||||||
27758|Dargalong Metamorphics|40892|5|Briefly described|p71|||Mention Fig.2||||||
27758|Dargalong Metamorphics|40918|5|Briefly described|p101|||||||||
27758|Dargalong Metamorphics|41465|6|Mentioned|p14|||||||||
27758|Dargalong Metamorphics|42304|6|Mentioned|p14||Precambrian|||||||
27758|Dargalong Metamorphics|42500|5|Briefly described|p15|||||||||
27758|Dargalong Metamorphics|42502|5|Briefly described|p2|||||||||
27758|Dargalong Metamorphics|42620|3|Fully described|p27|||Age uncertain||||||
27758|Dargalong Metamorphics|42658|5|Briefly described|p21|||Precambrian||||||
27758|Dargalong Metamorphics|42681|6|Mentioned|p17|||||||||
27758|Dargalong Metamorphics|42691|5|Briefly described|map legend|Precambrian||||||||
27758|Dargalong Metamorphics|42765|5|Briefly described|p18|||see also P21||||||
27758|Dargalong Metamorphics|43060|3|Fully described|p20,Table 1c|||Proterozoic age||||||
27758|Dargalong Metamorphics|43083|3|Fully described|p16, p17 Tb 1|||Unconformable below Pratt and Mitchell River Volcanics ans Gilbert Formation; gradational contact with McDevitt Metamorphics. Prob.Early Proterozoic age. Biotite gneiss, amphibolite, schist and quartzite, mylonitic gneiss - detailed lithology included.||||||17-JUN-09
27758|Dargalong Metamorphics|43087|5|Briefly described|Fig.3, Fig.4|||||||||
27758|Dargalong Metamorphics|43110|5|Briefly described|Table 1.|||||||||
27758|Dargalong Metamorphics|43124|5|Briefly described|p28|||||||||
27758|Dargalong Metamorphics|43254|5|Briefly described|map legend||Mesoproterozoic|of Yambo Metamorphic Group.||||||
27758|Dargalong Metamorphics|43285|5|Briefly described|Map Legend|||age Middle Proterozoic.||||||
27758|Dargalong Metamorphics|43287|6|Mentioned|Map Legend||Paleozoic|||||||07-NOV-08
27758|Dargalong Metamorphics|43596|6|Mentioned|p8|||Formerly included rocks of the Yambo Metamorphic Group but subsequently found to comprise only two mappable units of schist and gneiss, excluding these rocks.||||||25-AUG-08
27758|Dargalong Metamorphics|43625|3|Fully described|p10||Mesoproterozoic|||||||
27758|Dargalong Metamorphics|43665|5|Briefly described|p14||Proterozoic|||||||
27758|Dargalong Metamorphics|43896|14|Not recorded|Map Legend||Proterozoic|||||||
27758|Dargalong Metamorphics|43898|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
27758|Dargalong Metamorphics|43901|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
27758|Dargalong Metamorphics|43902|14|Not recorded|p116,Fig.16,118|||||||||
27758|Dargalong Metamorphics|43904|14|Not recorded|Map Legend|||Archean?||||||
27758|Dargalong Metamorphics|44025|4|Described|p345,347,351|||Age 1044 my.||||||
27758|Dargalong Metamorphics|44043|14|Not recorded|p66,67,73,74|||||||||
27758|Dargalong Metamorphics|44091|14|Not recorded|p11||Paleoproterozoic|||||||07-NOV-08
27758|Dargalong Metamorphics|44246|5|Briefly described|Map Legend||Proterozoic|||||||
27758|Dargalong Metamorphics|44251|14|Not recorded|p1||Precambrian|||||||
27758|Dargalong Metamorphics|44258|14|Not recorded|p31,29||Archean|||||||07-NOV-08
27758|Dargalong Metamorphics|44292|14|Not recorded|p14,17|||||||||
27758|Dargalong Metamorphics|44293|14|Not recorded|Map Legend||Proterozoic|||||||
27758|Dargalong Metamorphics|44294|2|Defined|Tb.2,opp.p10,map|||||||||
27758|Dargalong Metamorphics|44296|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
27758|Dargalong Metamorphics|44425|14|Not recorded|p3,8,10-12,22,map|||||||||
27758|Dargalong Metamorphics|44843|14|Not recorded|p179|||||||||
27758|Dargalong Metamorphics|44926|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27758|Dargalong Metamorphics|45003|14|Not recorded|p60|||||||||
27758|Dargalong Metamorphics|45008|14|Not recorded|p11-108|||Radiometric age is not younger than Mesoproterozoic.||||||
27758|Dargalong Metamorphics|45025|2|Defined|p20-3||Precambrian|||||||
27758|Dargalong Metamorphics|45065|6|Mentioned|p16|||||||||
27758|Dargalong Metamorphics|45076|3|Fully described|p78|||||||||
27758|Dargalong Metamorphics|60087|5|Briefly described|Map legend|Proterozoic|Proterozoic|Gneiss, quartzite, amphibolite, schist.||||||
27758|Dargalong Metamorphics|60425|6|Mentioned|p51 Tb. 3|||Unconformably overlain by Pratt Volcanics.||||||07-FEB-11
27758|Dargalong Metamorphics|61527|5|Briefly described|p790 Fig.1|Proterozoic|Proterozoic|||||||
27758|Dargalong Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.|1642 +/- 7 Ma (maximum depositional age).|||||
27758|Dargalong Metamorphics|68337|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Etheridge Province.|||Includes Cardross Orthogneiss.||Grey, foliated, porphyroclastic gneiss, augen gneiss, sillimanite-garnet biotite gneiss; minor foliated amphibolite; foliated biotite granite to granodiorite, gneissic (muscovite)-biotite granite, granitic gneiss.|
27758|Dargalong Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||||Is overlain conformably by Robertson River Subgroup.||
27758|Dargalong Metamorphics|68576|5|Briefly described|Q_11: p14, p16-17|Mesoproterozoic|Paleoproterozoic||||||Porphyroclastic gneiss, augen gneiss, sillimanite-biotite gneiss and minor amphibolite. Siliceous mylonite with relict feldspar porphyroclasts occurs locally adjacent to the Palmerville Fault (Tasman Line).|
27758|Dargalong Metamorphics|69591|5|Briefly described|p65-66, p70-71|||Dargalong Inlier, Yambo Subprovince. A variety of complexly intermixed rocks. Previously included rocks of the Yambo Metamorphic Group. Deposition age is uncertain. The augen gneiss is assigned to the Cardross Orthogneiss, which is geochemically similar to I-type granodiorite. Appears to grade into McDevitt Metamorphics. See also reference to [superseded] Dargalong Metamorphic Group (p61, p70).||||Adjacent to McDevitt Metamorphics.|Banded migmatitic gneiss, augen gneiss, amphibolite (metamorphosed dolerite sills and/or dykes; some intercalated mafic volcanics), with some medium to coarse schist and scattered quartzite lenses and minor calc-silicate gneiss.|
27758|Dargalong Metamorphics|70207|6|Mentioned|p74|Mesoproterozoic|Paleoproterozoic|||||||
27758|Dargalong Metamorphics|70345|6|Mentioned|p3|Mesoproterozoic|Palaeoproterozoic|||||||
27758|Dargalong Metamorphics|70673|6|Mentioned|p7|||Age range given as Paleoproterozoic-Mesoproterozoic.||||||
27758|Dargalong Metamorphics|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1580+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
27758|Dargalong Metamorphics|71792|5|Briefly described|p5|||Coen Inlier. Rocks previously assigned to this unit by Whitaker & Willmott, 1968 have since been recognised as belonging to the Coen Metamorphic Group.||||||
27758|Dargalong Metamorphics|72983|6|Mentioned|p15|Mesoproterozoic|Paleoproterozoic|||||||
27758|Dargalong Metamorphics|73083|6|Mentioned|p76|||||||||
73021|Dark Dog Limestone|63152|5|Briefly described|p120 Fig. 3|||Of the Jack Group (Graveyard Creek Supergroup). Overlain by Red Bull Formation. Shallow marine (including shoal and tidal channel deposits).||||||10-APR-07
75641|Dartmoor Granodiorite|68679|5|Briefly described|p361, p366 Fig.5.57|Permian|Permian|Northern Connors Subprovince. Early Permian. REE plot.|289 +/- 2.0 Ma (U-Pb SHRIMP: Cross et al. 2012).|||||
75641|Dartmoor Granodiorite|68901|5|Briefly described|p4, p81-p83, p146|||Northern New England Orogen, Bowen Region. Forms hilly country but is generally poorly exposed. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|289 +/- 2.0 (SHRIMP U-Pb)||||Pale-pinkish grey, fine-grained, slightly porphyritic hornblende-biotite granodiorite, characterised by a well developed granophyric texture and numerous small plagioclase phenocrysts.|15-NOV-18
75641|Dartmoor Granodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|289+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
75641|Dartmoor Granodiorite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pinkish grey to pale pink, fine to medium-grained, uneven-grained to slightly porphyritic biotite and hornblende-biotite granodiorite to biotite-hornblende quartz monzodiorite; commonly granophyric.|
77680|David Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pale pinkish-grey, medium-grained, porphyritic hornblende-biotite monzogranite; with scattered mafic inclusions to ~10 cm (most < 3 cm across).|
77680|David Granite|68576|5|Briefly described|Q_11: p13|||East of Almaden township. Forms large outcrops.|c.301 Ma (Rb-Sr).|Ootann Supersuite.|||White-pink, sparsely enclave-bearing, seriate, medium- to coarse-grained biotite monzogranite. Enclaves are grey, equigranular to sparsely porphyritic, biotite-plagioclase with a microdioritic texture, to 15cm.  Minor thin biotite aplite veins.|
79120|Dawn Formation|70913|2|Defined|p1, p8 fig 3, p11, p44-p58, p67 fig 9|Permian|Permian|Gympie Province. New name. Replaces the Alma Formation, Alma unit. Equivalent to tuff and shale members of Third Slate Group of Dunstan (1911). Representative section and drill holes are named. Distribution is briefly discussed. Ranges from 50 to 200m thick. See also p79, p87,  App 1 maps.|~302 Ma (Maximum depositional age, U-Pb zircon)|Gympie Group|Includes the Kidgell Andesite Member, Hall Clastics Member, Ellen Harkins Shale Bed and Excelsior Marker Bed.|Overlies the Highbury Basalt. Overlain by the Mary and Tozer Basalts. Is intruded by the Tozer Basalt Member.|Pale green tuffaceous siltstone, mudstone, dacitic tuff, minor sandstone, ignimbrite and rare dacite flows that are in part silicified.|15-SEP-17
79120|Dawn Formation|73303|5|Briefly described|p61 Fig.2, p62|Cisuralian|Cisuralian|New England Orogen. Gympie Terrane, southern. Brachiopod assemblage correlative with Kolbar Formation.|302 Ma detrital zircon maximum depositional age|||Overlies Highbury Basalt, underlies Mary Basalt.|Dominated by fine- to coarse-grained volcaniclastic rocks.|
40114|Dawson Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgda].  Granite.||||||
40114|Dawson Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to grey, and locally cream to white, medium to coarse, equigranular to slightly porphyritic, hornblende-biotite and biotite granite.||||||
40114|Dawson Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
40114|Dawson Granite|65388|4|Described|p248-249, p236 Fig. 81, p237, 238|Early Permian|Late Carboniferous|Intrudes Torsdale Volcanics. Interpreted to post-date the Okangal and Hainault Granodiorites, Pinedale and Jonah Vale Granites, Montour Gabbro, Glen View Quartz Monzodiorite, Wind Mill Diorite. Age uncertain.  Pale pink, medium-grained, slightly porphyritic biotite monzogranite||||||
40114|Dawson Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age tentative: intruded by Carboniferous-Permian units and postdates a number of Carboniferous-early Permian intrusives (listed).||||Intrudes Torsdale Volcanics.|Pale pink, leucocratic, medium-grained, slightly porphyritic biotite monzogranite with alkali feldspar phenocrysts.|
28498|Dawson Range Sandstone|39212|6|Mentioned|p15|||||||||
28498|Dawson Range Sandstone|39445|5|Briefly described|Table 9|||||||||
28498|Dawson Range Sandstone|39491|6|Mentioned|p24|||||||||
28498|Dawson Range Sandstone|45095|6|Mentioned|p55|||Refers Reid (1945)||||||
79157|Dead Horse Gneiss|68679|5|Briefly described|p360, p362, p369|||Northern Connors Subprovince. Zircons and monazites record a significant high-grade metamorphic event or events at ~298-291 Ma. Age determination elaborated on p362.|298.9 +/- 3.3 Ma (U-Pb SHRIMP: Cross et al. 2012).|||||
79157|Dead Horse Gneiss|68901|5|Briefly described|p4, p30, p57-p60, p145|Permian||northern New England Orogen, Bowen Region. Informal name. SHRIMP age is interpreted as the age of metamorphism. SHRIMP results and analysis discussed in detail.|298.9 +/- 3.3 Ma (SHRIMP U-Pb)||||Medium-grained, quartz-feldpsar-muscovite-biotite gneiss.|28-SEP-18
79157|Dead Horse Gneiss|69952|6|Mentioned|p86|||A metamorphic age of 298.9 +/- 3.3 Ma (Cross et al., 2012) is within error of the age of the adjacent Pickhandle Tonalite (297.1 +/- 2.0 Ma), implying granitoid emplacement and metamorphism were part of the same event.||||||
79157|Dead Horse Gneiss|70673|5|Briefly described|p5, p118|||Part of the Urannah Batholith. Age of a metamorphic event. Has well-developed foliation.|298.9 +/- 3.3 Ma (Cross et al., 2012).|||||
27080|Dead Horse Metabasalt|22963|5|Briefly described|p69||Paleoproterozoic|||||||07-NOV-08
27080|Dead Horse Metabasalt|23220|5|Briefly described|Fig.2 p10|||Geochemically similar to Cobbold Metadolerite. Of Robertson River Subgroup.||||||27-MAY-15
27080|Dead Horse Metabasalt|23291|4|Described|p86, Tb. 3.6, p23|Paleoproterozoic|Paleoproterozoic|Parent: Robertson River Subgroup. Underlying Unit: Daniel Creek Formation. Geological Province: Georgetown Region.||||||27-MAY-15
27080|Dead Horse Metabasalt|23430|6|Mentioned|p450|||||||||
27080|Dead Horse Metabasalt|23616|5|Briefly described|p27|||Of Robertson River Subgroup of the Etheridge Group.||||||
27080|Dead Horse Metabasalt|38714|1|Redefined|p186|Mesoproterozoic|Mesoproterozoic|Supersedes Dead Horse Metabasalt Member.||||||
27080|Dead Horse Metabasalt|39566|6|Mentioned|p51|||||||||
27080|Dead Horse Metabasalt|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27080|Dead Horse Metabasalt|39924|4|Described|p341|||||||||
27080|Dead Horse Metabasalt|41272|5|Briefly described|M 1of1 H06|||||||||
27080|Dead Horse Metabasalt|41975|6|Mentioned|p435|||||||||
27080|Dead Horse Metabasalt|42199|5|Briefly described|Table 1 P280|||||||||
27080|Dead Horse Metabasalt|42691|5|Briefly described|map legend|Precambrian||||||||
27080|Dead Horse Metabasalt|43060|6|Mentioned|p34|||of Robertson River Subgroup||||||
27080|Dead Horse Metabasalt|43664|4|Described|p25|||||||||
27080|Dead Horse Metabasalt|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
27080|Dead Horse Metabasalt|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Overlies: Daniel Creek Formation. Intruded by Cobbold Metadolerite. Underlies: Corbett Formation.||||||27-MAY-15
27080|Dead Horse Metabasalt|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group). Conformably overlies Daniel Creek Formation. Conformably overlain by Corbett Formation. Intruded by Cobbold Metadolerite.||||||07-NOV-08
27080|Dead Horse Metabasalt|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||19-AUG-04
27080|Dead Horse Metabasalt|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
27080|Dead Horse Metabasalt|64250|6|Mentioned|p25 fig 10|||Georgetown Block.||Unit in Etheridge Group.||||
27080|Dead Horse Metabasalt|65887|4|Described|p39-53|Statherian|Statherian|Of Robertson River Subgroup. Overlies Daniel Creek Formation. Overlain by Corbett Formation. Conformable. 1000m thick. Fine- to coarse-grained tholeiitic basalts and pillow lavas, and minor interbedded sediments. LA-ICPMS U-Pb zircon age 1663+/-13 Ma.||||||
27080|Dead Horse Metabasalt|66800|5|Briefly described|p926 Table 1, p928, pp932-933.||||Probably 1674.9 +/- 3.3 Ma.|Unit in Robertson River Subgroup.||Overlies Daniel Creek Formation. Is overlain by Corbett Formation.||
27080|Dead Horse Metabasalt|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Georgetown-Coen-Yambo Inliers.|Emplaced 1663 +/- 13 Ma (LA-ICPMS zircon).|Lower Etheridge Group.||||
27080|Dead Horse Metabasalt|67341|5|Briefly described|vi, p10|||Forsayth Subprovince, Etheridge Province.||||Overlies Daniel Creek Formation. Is overlain by Corbett Formation.||
27080|Dead Horse Metabasalt|67430|6|Mentioned|p25|||||||||
27080|Dead Horse Metabasalt|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Conformably overlies Daniel Creek Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Corbett Formation.|Foliated amphibolite grading into aphyric metabasalt with local pillows, hyaloclastic breccia and amygdales, minor mafic schist and quartzite; metabasalt, locally pillowed, minor metadolerite and metagabbro (unmapped) and interbedded siltstone.|
27080|Dead Horse Metabasalt|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. Low K, Th and U radiometric responses.||Unit in Robertson River Subgroup.||Conformably overlies Daniel Creek Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Corbett Formation.|Metabasalt, locally pillowed, hyaloclastic and/or amygdaloidal; minor metadolerite and metagabbro (unmapped) and interbedded siltstone.|
27080|Dead Horse Metabasalt|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Of the Robertson River Subgroup.||Intruded by the Cobbold Metadolerite. Conformably overlies Daniel Creek Formation. Is overlain conformably by Corbett Formation.|Metabasalt, locally pillowed, hyaloclastic and/or amygdaloidal; minor metadolerite, and metagabbro (unmapped) and interbedded siltstone.|
27080|Dead Horse Metabasalt|69591|4|Described|p61-62, p64-65, p67-68, p108|Paleoproterozoic|Paleoproterozoic|Forsayth Subprovince, Etheridge Province. Lava compositions are typical of relatively evolved, low-K, Fe-rich continental (rift) tholeiites, with striking similarities to mafic sills in Curnamona Province (NSW) and dolerites of the Soldiers Cap Group.|1663 +/- 13 Ma (Baker et al., 2010).|Robertson River Subgroup.||Overlies Daniel Creek Formation. Is overlain by Corbett Formation.|Fine, dark green, aphyric metabasalt flows locally grading to fine, well-foliated amphibolite; minor interbeds of mudstone, siltstone, and quartzite (some of which may be metachert); pillow lavas, amygdales and hyaloclastic breccias common.|
27080|Dead Horse Metabasalt|71799|4|Described|p150 fig 2, p153 tbl 1|Statherian|Statherian|Georgetown area. Ages included SHRIMP and ICPMS dates [not specified which are which] that includes: 1675+/- 3 Ma-1656 +/- 2 Ma (sills and dykes), 1663 +/- 3 Ma (basaltic flows). Ages are derived from Baker et al, 2010; Black et al, 1998; Black et al, 2005; Neumann and Kositcin, 2011. Alteration is briefly mentioned. See also p155 fig 4, p156, p157 fig 5, p158, p165.|1663 +/- 14 Ma (Baker et al, 2010)|||Overlies the Daniel Creek Formation. Overlain by the Lane Creek and Corbett formations.|Low-k tholeiitic basalts to basaltic andesite.|03-OCT-18
27080|Dead Horse Metabasalt|73642|5|Briefly described|p10 Fig.8|Statherian|Statherian||1663+/-26 Ma|||||
26262|Deane Granodiorite|22847|3|Fully described|p 55|Early Devonian||||||||
26262|Deane Granodiorite|23422|5|Briefly described|p176, p214 Table 6.8|Early Devonian|Late Silurian|Of Deane Supersuite.||||||
26262|Deane Granodiorite|23430|5|Briefly described|Table 14.2 p460.||Silurian|See also p480. K-Ar; Rb-Sr age 411+/-2 Ma and 409+/-2 Ma.  Ravenswood Batholith Province.||||||
26262|Deane Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26262|Deane Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 191. I-Type.||||||
26262|Deane Granodiorite|42633|5|Briefly described|Table 1 P7|||Reserved||||||
26262|Deane Granodiorite|42750|2|Defined|p43|Early Devonian|Late Silurian|age of 411 +/- 2 Ma.||||||
26262|Deane Granodiorite|43093|4|Described|Appendix 1|||Rb/Sr age of 411+/-2Ma.||||||
26262|Deane Granodiorite|43259|4|Described|Appendix 1,p29.|Early Devonian|Late Silurian|Rb-Sr biotite age is 411+/-2 Ma.||||||
26262|Deane Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26262|Deane Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26262|Deane Granodiorite|62075|6|Mentioned|p15 Fig.7|Early Devonian|Late Silurian|Ravenswood batholith. Appears as Deane granodiorite.||||||
26262|Deane Granodiorite|62521|5|Briefly described|p7 Tb. 1, p18-19, p59|||Of Deane Supersuite (not Suite, due to var. in source rock chemistry). Age:411+/-2Ma(Rb-Sr).Zoned pluton - outer hornblende-biotite monzodiorite to qtz near margins/hornblende-biotite granite near core; trondhjemite core - roughly circular; age:409+/-2Ma.||||||14-JAN-08
26262|Deane Granodiorite|68731|6|Mentioned|p150|||||||||
26262|Deane Granodiorite|69592|5|Briefly described|p293-294|||Ravenswood Batholith, Charters Towers Province. Well-defined gravity lows suggest deep-seated, steep-sided plutons.||Deane Supersuite.|||A large concentrically-zoned pluton with a trondhjemite core that was not produced by fractional crystallisation of the rest of the pluton.|
34674|Deane Supersuite|22847|5|Briefly described|p 13|||||||||
34674|Deane Supersuite|23422|4|Described|p176, p214 Table 6.8|Early Devonian|Late Silurian|||||||
34674|Deane Supersuite|62521|4|Described|p53, p59|Devonian|Silurian|Contains Deane Granodiorite. Geological Province: Ravenswood Batholith. Large complex pluton of granite, granodiorite, tonalite and trondhjemite.||||||21-DEC-07
34674|Deane Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Millchester, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
34674|Deane Supersuite|69592|6|Mentioned|p293|||Ravenswood Batholith, Charters Towers Province.|||Deane Granodiorite.|||
36496|Deans Gorge Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 128.||||||
38869|Deception Quartz Monzonite|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38869|Deception Quartz Monzonite|24615|5|Briefly described|CD|Triassic|Triassic|[Rggd].  Pink fine- to medium-grained hornblende-biotite quartz monzonite and granite with granophyric groundmass and miarolitic cavities.||||||
38869|Deception Quartz Monzonite|67203|5|Briefly described|p7|Triassic|Triassic|Despite slightly younger K-Ar ages (Webb and McDougall, 1968), intrusive relationships indicate that this unit (and Rule Gabbro, Lawyer Granite) is marginally older than the Robert Granite (230.2+/-3.7Ma), and therefore broadly contemporaneous with the Bobby Volcanics, Agnes Water Volcanics and other granitoids further east.||Unit in Glassford Igneous Complex.||Intrudes Bobby Volcanics.|Dominantly high-level (miarolitic and granophyric), leucocratic, alkali-rich granites to quartz monzonites and small gabbro bodies.|12-NOV-15
38869|Deception Quartz Monzonite|68008|2|Defined|p140, p405, p407-408, p410-411|Late Triassic|Late Triassic|The type area is along Deception Creek, after which the unit is named, below the junction of its two main tributaries and upstream along the northern tributary. Covers a roughly triangular area 2km across, 8km WSW of Many Peaks township. Forms steep, dissected topography. Geophysics described. Age from correlation.||Glassford Igneous Complex.||Intrudes Rule Gabbro. Is intruded by Lawyer Granite. Correlated with Robert Granite.|Pink, medium-grained, equigranular, leucocratic hornblende-biotite quartz monzonite to granite. Has micrographic textures and miarolitic cavities, some filled with secondary minerals, indicating shallow depth of intrusion.|
38869|Deception Quartz Monzonite|68679|5|Briefly described|p431-432|||Bundaberg-Agnes Water-Biloela region.||Glassford Igneous Complex.|||Pink fine- to medium-grained hornblende-biotite quartz monzonite and granite with granophyric groundmass and miarolitic cavities.|
38869|Deception Quartz Monzonite|73450|6|Mentioned|p11|||||||||
36613|Deep Creek granite|23291|4|Described|p99 Tb. 3.11|Carboniferous|Carboniferous|Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36613|Deep Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 414.  I-Type.||||||
36375|Dehn Coal Measures|23425|5|Briefly described|p373 Fig 9.10|||Of Pascoe River Group.||||||
77829|Delubra Gabbro|65388|2|Defined|p311-313, p46, 301, 302, 305, 306|Late Permian|Late Permian|Name modifed from Delubra Quartz Gabbro and use restricted to largest of 7 bodies of original description of Whitaker & others (1974), but also includes adjoining body which was previously called Hawkwood Gabbro. Intrudes Narayen beds. Intruded by the Cheltenham Creek Granite. Maybe emplaced at same time as Cadarga Creek Granodiorite.  Unconformably overlain by Evergreen Formation. New Ar/Ar age 261+/- 6 (hornblende). Ar/Ar ages 257+/-10 Ma (Hb), 253+/-10Ma (biotite) reported to be from Pollard Granodiorite are probably from this unit. Medium to coarse-grained gabbro characterised by abundant equant hornblende crystals. See also p321, 329, 330, 340.||||||
77829|Delubra Gabbro|68008|6|Mentioned|p435|||Rawbelle Batholith. May have undergone magma mingling with the adjacent Cadarga Creek Granodiorite.||||||
77829|Delubra Gabbro|68553|6|Mentioned|Map legend; schematic diagram.|Early Triassic|Late Permian|This unit, as well as the Harrami Igneous Complex, the Tandora and Wingfield Suites, and various unnamed plutonic units in the Rawbelle Batholith, are all mapped under the symbol, PRgr.||||||30-SEP-15
77829|Delubra Gabbro|68679|5|Briefly described|p312, p416, p418-419|Early Triassic|Permian|Rawbelle Batholith, northern New England Orogen. Outcrop area ~140 km2. May form a complex with Cadarga Creek Granodiorite and Hawkwood Gabbro. Includes Hawkwood Gabbro of Whitaker et al. (1974). Compositional diversity attributed to two-stage fractional crystallisation. Commonly net-veined; rhythmic layering well-developed in the north. Several age determinations given.|c.261 Ma to c.247 Ma.|||Intrudes Narayen beds.Is intruded by Cheltenham Creek Granite.|Medium-K, calc-alkaline: gabbro, with subordinate quartz diorite and granodiorite; in the south, mainly layered gabbro comprising leucogabbro, pyroxenite and ferrogabbro; also irregular masses of diorite and locally abundant rafts of metasediments.|
41092|Delusion Granodiorite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41092|Delusion Granodiorite|65388|4|Described|p249-250, p243, p236 Fig. 81|Early Permian|Late Carboniferous|Intrudes Torsdale Volcanics. Grey, fine-grained, highly porphyritic, biotite-hornblende granodiorite||||||
41092|Delusion Granodiorite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age is tentative.||||Intrudes Torsdale Volcanics.|Fine-grained, highly porphyritic, biotite-hornblende granodiorite. Large inclusions of volcanics near contacts.|
24242|Democrat Rhyolite Member|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Idalia Rhyolite (Croydon Volcanic Group).  Recrystallised crystal-rich rhyolitic ignimbrite.||||||
24242|Democrat Rhyolite Member|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Idalia Rhyolite (Croydon Volcanic Group).||||||02-JUL-04
24242|Democrat Rhyolite Member|23291|5|Briefly described|p26|Mesoproterozoic|Mesoproterozoic|Parent: Idalia Rhyolite. Geological Province: Georgetown Region.||||||15-APR-15
24242|Democrat Rhyolite Member|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V806. S-Type.||||||
24242|Democrat Rhyolite Member|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24242|Democrat Rhyolite Member|40659|2|Defined|p250|Mesoproterozoic|Mesoproterozoic|Of Idalia Rhyolite.||||||21-JUN-04
24242|Democrat Rhyolite Member|40954|6|Mentioned|p132|||||||||
24242|Democrat Rhyolite Member|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24242|Democrat Rhyolite Member|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24242|Democrat Rhyolite Member|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Idalia Rhyolite (Croydon Volcanic Group).  Recrystallised crystal-rich rhyolitic ignimbrite.||||||
24242|Democrat Rhyolite Member|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Dark grey recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68416|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province. Shown as younger than D2 ~ 1552 Ma.|< 1552 Ma|Of the Idalia Rhyolite.|||Dark grey, recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
24242|Democrat Rhyolite Member|68417|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province.||Of the Idalia Rhyolite.|||Dark grey, recrystallised moderately crystal-rich rhyolitic to rhyodacitic(?) ignimbrite; porphyritic rhyolite (intrusive?); disseminated graphite, some graphite pellets; garnet present in some rocks.|
23543|Denford Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||01-JUN-09
23543|Denford Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 273. I-Type.||||||
23543|Denford Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
23543|Denford Granite|41235|6|Mentioned|Fig.2a|||||||||
23543|Denford Granite|41740|6|Mentioned|p222|||||||||
23543|Denford Granite|43259|4|Described|Appendix 1,p35.||Carboniferous|||||||
23543|Denford Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Age: ~315-313Ma. Pale pink, fine-grained, slightly porphyritic to seriate or pegmatitic, granophyric (tourmaline-topaz-) biotite granite; with associated Sn mineralisation. I-type.||||||07-FEB-11
24914|Denny Gully Member|30451|4|Described|p16]|||See also Fig.2||||||
24914|Denny Gully Member|31999|5|Briefly described|p149|||Table 1||||||
24914|Denny Gully Member|32140|6|Mentioned|p9|||Dev. Mb. Dawes Range Fm.||||||
24914|Denny Gully Member|32865|6|Mentioned|p479|||Davies Range Fm. Fauna||||||
24914|Denny Gully Member|44379|2|Defined|p3-7,Tb.1,3,map|||Unit of Dawes Range Formation.||||||
36219|Depression Basalt|23502|5|Briefly described|Map Legend||Pleistocene|of McBride Basalt Group.||||||
36219|Depression Basalt|23503|5|Briefly described|Map Legend||Pleistocene|of McBride Basalt Group.||||||
36219|Depression Basalt|23624|4|Described|p27|||Geological Province: McBride Province.||||||30-JUN-15
36219|Depression Basalt|68330|5|Briefly described|Map legend.|Pleistocene|Pleistocene|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
36219|Depression Basalt|68331|5|Briefly described|Map legend.|Pleistocene|Pleistocene|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
36219|Depression Basalt|68576|6|Mentioned|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
36219|Depression Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pliocene|Pliocene|McBride Basalt Province.|2.6 Ma|||||
27140|Desailly Granite|23423|6|Mentioned|p238|||||||||
27140|Desailly Granite|23430|5|Briefly described|p499|||Kennedy Province||||||
27140|Desailly Granite|42304|2|Defined|p24|Permian|Carboniferous|Reserved as Mount Desailly Granite.||||||
27140|Desailly Granite|42968|5|Briefly described|Fig.1,p91|||See also misspelling - as Desailley Granite.||||||01-JUN-09
27140|Desailly Granite|43625|5|Briefly described|p124,Appendix 6|||||||||
27140|Desailly Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
27140|Desailly Granite|60425|4|Described|p72, p181, p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla S'suite). S-Type. Muscovite-biotite with biotite-rich gneissic inclusions; minor scheelite in qtz veins + alteration zones; pronounced north-westerly and northerly elongations. Geol.prov: Kennedy Prov. Lith.details included||||||07-FEB-11
27140|Desailly Granite|66852|6|Mentioned|pp937-938, p940 Fig.4.|||Shows evidence of syntectonic emplacement.||Unit in Whypalla Supersuite.||||
27140|Desailly Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Curraghmore Suite.||||
77813|Desert Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Porphyritic biotite granite; hydrothermally altered porphyritic biotite granite.|
37880|Desert Creek Suite|23291|5|Briefly described|p96 Tb. 3.11, p100 Tb. 3.12|Late Carboniferous|Late Carboniferous|Parent: O'Brien's Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
75626|Devlins Pocket Quartz Diorite|69594|5|Briefly described|p567 Fig.7.39, p570, p571 Figs.7.45-46|Cretaceous|Cretaceous|Northern Bowen Basin. Geochemical plots and discussion.||||||
75626|Devlins Pocket Quartz Diorite|73036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Pale grey, fine to medium-grained, uneven-grained to slightly porphyritic (clinopyroxene-) biotite-hornblende quartz diorite, with locally abundant mafic inclusions.|
36263|Devon Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36263|Devon Microgranite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36263|Devon Microgranite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Slightly porphyritic biotite microgranite; included in Nettle Granite on most maps. I-type.||||||07-FEB-11
70415|Diamond Hill Granite|65452|6|Mentioned|p6 Fig.2|Permian|Permian|||||||
70415|Diamond Hill Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Mostly decomposed medium to coarse-grained biotite granite (syenogranite) with abundant microgranite and rhyolite dykes.|
70415|Diamond Hill Granite|68679|5|Briefly described|p410, p421-422|Guadalupian|Guadalupian|Gayndah-Gladstone belt, southern part of the northern New England Orogen.|||||Biotite granite (syenogranite?), abundant microgranite, rhyolite dykes; weak to moderate foliation.|
70415|Diamond Hill Granite|73036|5|Briefly described|Map legend|Late Permian|Late Permian||||||Mostly decomposed, medium to coarse-grained biotite granite (syenogranite?) with abundant microgranite and rhyolite dyke.|
69499|Dickie Hill Granite|68330|5|Briefly described|Map legend.|Permian|Late Carboniferous|Kennedy Province.|||||Pink, fine-grained porphyritic biotite granite with quartz and feldspar phenocrysts and common miarolitic cavities.|
69499|Dickie Hill Granite|68331|5|Briefly described|Map legend.|Permian|Late Carboniferous|Kennedy Province.|||||Pink, fine-grained porphyritic biotite granite with quartz and feldspar phenocrysts and common miarolitic cavities.|
36281|Dickson Creek Rhyolite|23291|4|Described|p93 Fig. 3.9|Early Permian|Late Carboniferous|Parent: Bulleringa Volcanic Subgroup. Age: 289+/-2Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36281|Dickson Creek Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Bulleringa Volcanic Subgroup, Scardons Volcanic Group.||||||
36281|Dickson Creek Rhyolite|23616|5|Briefly described|Table 3 p52|Early Permian|Late Carboniferous|Of Scardons Volcanic Group. Dargalong Province.||||||
36281|Dickson Creek Rhyolite|68405|5|Briefly described|Map Legend|Cisuralian|Cisuralian|Kennedy Province.|~ 290 Ma|Of the Bulleringa Volcanic Subgroup.|||Pink to grey, lithics poor, crystal-rich to very crystal-rich, rhyolitic ignimbrite; basal lithics-rich layer with clasts of granite and granodiorite.|
33887|Dido Supersuite|22533|6|Mentioned|p54|Early Devonian|Silurian|placed in Pama Province||||||
33887|Dido Supersuite|23291|3|Fully described|p36,p90 Tb. 3.8|Early Devonian|Silurian|Geological Province: Dido Batholith.||||||08-JUL-15
33887|Dido Supersuite|23430|5|Briefly described|p485|||Pama Province||||||
33887|Dido Supersuite|63154|5|Briefly described|p285 Fig. 5|Silurian|Silurian|Geological province: Georgetown Inlier.||||||11-APR-07
33887|Dido Supersuite|67848|5|Briefly described|p8.|Late Silurian|Late Silurian|Georgetown Province. Granitoids.|<431 Ma (Bain and Draper 1997).|||||
33887|Dido Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Etheridge Province. This unit, the Mount Webster and White Springs Supersuites, and various ungrouped Silurian plutonic units, are all mapped under the same symbol, Sg.||||||
33887|Dido Supersuite|69592|5|Briefly described|p280-281, p283-285, p289-290, p297|Silurian|Silurian|Dido and Copperfield Batholiths. Geochemistry described in some detail; similar to the Craigie Supersuite in the Reedy Springs Batholith. Includes a component of the Oak River Granodiorite on geochemical grounds. Crustal evolution discussed.|c.431 Ma.||Christmas Hill Trondhjemite; Dido, Emma Creek Tonalites; Oak River, Watch Hill Granodiorites.||Grey biotite tonalite to granodiorite, biotite trondhjemite or leucotonalite, hornblende-biotite and hornblende tonalite; minor (augite-)biotite-hornblende quartz diorite and diorite, biotite-muscovite granite; rare gabbro; commonly foliated.|
25715|Dido Tonalite|23032|4|Described|p37,38||Early Silurian|U/Pb Age: 431+10-20 Ma.||||||
25715|Dido Tonalite|23074|5|Briefly described|p739|Silurian|Silurian|||||||
25715|Dido Tonalite|23291|4|Described|p36,p90 Tb. 3.8|Early Devonian|Silurian|Age: 431+/-7Ma (SHRIMP). Parent: Dido Supersuite. Geological Province: Dido Batholith.||||||23-MAR-15
25715|Dido Tonalite|23424|5|Briefly described|Table 8.1 p346.||Silurian|Faulted against Wando Vale Subgroup. Age: U-Pb zircon age of 431+/-15 Ma.||||||
25715|Dido Tonalite|23430|5|Briefly described|p469||Silurian|Also see p460 Table 14.2. K-Ar; Rb-Sr 395-400 Ma. Zircon crystallisation 431 +/- 7 Ma. Pama Province.||||||
25715|Dido Tonalite|23431|6|Mentioned|p532|||||||||
25715|Dido Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 68. I-Type.||||||
25715|Dido Tonalite|23616|6|Mentioned|p67|||||||||
25715|Dido Tonalite|23619|4|Described|p41 Table 2||Early Silurian|Intrudes Einasleigh and Halls Reward Metamorphics and Balcooma Metavolcanics and Lugano Metamorphics. Also see p7. Overlying unit Bally Knob Volcanics and McBride Basalt Group. Georgetown Province.||||||
25715|Dido Tonalite|23713|5|Briefly described|p27||Early Silurian|Age: 431+10-21 Ma. Georgetown Province.||||||
25715|Dido Tonalite|41260|6|Mentioned|p125|||||||||
25715|Dido Tonalite|41675|1|Redefined|p60|Early Silurian||Modified name from Dido Granodiorite||||||
25715|Dido Tonalite|41679|6|Mentioned|p255|||||||||
25715|Dido Tonalite|41680|6|Mentioned|p104|||||||||
25715|Dido Tonalite|42054|6|Mentioned|p273|||||||||
25715|Dido Tonalite|42279|4|Described|p22|||See also Fig.3||||||
25715|Dido Tonalite|42692|5|Briefly described|map legend|Early Devonian|Silurian|||||||
25715|Dido Tonalite|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
25715|Dido Tonalite|42709|6|Mentioned|map legend|||||||||
25715|Dido Tonalite|42933|6|Mentioned|p221|||||||||
25715|Dido Tonalite|43060|5|Briefly described|p86|||||||||
25715|Dido Tonalite|43083|6|Mentioned|p117|||Geological province: Georgetown Province.||||||17-JUN-09
25715|Dido Tonalite|43113|4|Described|Table 2 p27||Early Silurian|Age 431 +10/-20 Ma (U-Pb zircon dating - Black & McCulloch, 1990)||||||
25715|Dido Tonalite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
25715|Dido Tonalite|43259|4|Described|Appendix 1,p19.|Early Devonian|Late Silurian|U-Pb zircon age is 430+10-20 Ma.||||||
25715|Dido Tonalite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
25715|Dido Tonalite|43480|6|Mentioned|58|||||||||
25715|Dido Tonalite|43664|6|Mentioned|p77|||||||||
25715|Dido Tonalite|43716|6|Mentioned|p116|||||||||
25715|Dido Tonalite|50200|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
25715|Dido Tonalite|50202|5|Briefly described|Map legend|Late Silurian|Late Silurian|Grey, foliated hornblende-biotite tonalite and quartz diorite, and granodiorite.||||||
25715|Dido Tonalite|67455|4|Described|p575 Table 1, p576, p577, p590.|Early Silurian|Early Silurian|The elongate pluton, and its weak to locally strong, steeply dipping foliation, trend northeast. Affected by Early Silurian contractional deformation. Forms the eastern boundary of the Balcooma domain, Greenvale Province.|431 +/- 7 Ma (U-Pb zircon: Bain et al. 1997).||||Biotite- and biotite-hornblende-bearing tonalite pluton.|
25715|Dido Tonalite|68336|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith. Five facies are mapped separately.|||||Mainly grey, foliated, hornblende-biotite tonalite and quartz diorite; olivine gabbro, hypersthene gabbro and troctolite.|
25715|Dido Tonalite|68341|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith. Five facies are mapped separately.|||||Mainly grey, foliated, hornblende-biotite tonalite and quartz diorite; olivine gabbro, hypersthene gabbro and troctolite.|
25715|Dido Tonalite|68344|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Dido Batholith, Thalanga Province. Four facies are mapped separately. Has low K, Th and U radiometric responses.|||||Grey, foliated hornblende-biotite tonalite, granodiorite and quartz diorite, minor muscovite pegmatite and aplite veins, enclaves and screens of gneiss and amphibole.|
25715|Dido Tonalite|68410|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Dido Batholith. The 4 variants are mapped separately.|||||Olivine gabbro, hypersthene gabbro and troctolite; biotite-clinopyroxene-hornblende quartz diorite and diorite; foliated hornblende-biotite tonalite and quartz diorite; foliated biotite and hornblende-biotite granodiorite or tonalite, leucogranite.|
25715|Dido Tonalite|68576|5|Briefly described|Q_11: p33|Early Silurian|Early Silurian|NNE-trending; locally 13 km wide. Strongly weathered; rarely exposed.||||Intrudes the Balcooma Metavolcanic Group.||
25715|Dido Tonalite|68731|6|Mentioned|p151 Fig 3.51, p153 Fig 3.53, p155, p157|Silurian|Silurian|||||Intrudes the Balcooma Metavolcanic Group, and the Ringwood Park Microgranite.||
25715|Dido Tonalite|69079|6|Mentioned|p60|Devonian|Silurian|||||Intrudes Lugano Metamorphics and Eland Metavolcanics (Lucky Creek Metamorphic Group).||
25715|Dido Tonalite|69592|5|Briefly described|p283-285|Silurian|Silurian|Dido Batholith. Geochemistry described. Champion (1991) recognised the composite character of this unit.|421 +/- 7 Ma (SHRIMP U-Pb zircon).|Dido Supersuite.|||(Eastern part): grey, biotite-clinopyroxene-hornblende quartz diorite and diorite; minor gabbro; commonly foliated. I-type.|
25715|Dido Tonalite|69952|5|Briefly described|p6, p104, p106|Early Silurian|Early Silurian|On p104, this age determination is attributed to Bain et al. (1997). Being within error of the age of the Lugano Metamorphics, there is the possibility that this unit intruded its own volcanic pile (represented by the Lugano Metamorphics).|431 +/- 7 Ma (Withnall and Hutton, 1997).|||Intrudes Lugano Metamorphics.||
25715|Dido Tonalite|70744|5|Briefly described|p947|Silurian|Silurian|Greenvale Province. Associated with Benambran Orogeny.|c.430 Ma (Hutton et al., 1997).|||||
25715|Dido Tonalite|70749|5|Briefly described|p43|Silurian|Silurian|Greenvale Province.|431 +/- 7 Ma.|||||
25715|Dido Tonalite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|431+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
25715|Dido Tonalite|71966|6|Mentioned|p990|Wenlock|Wenlock|Geological province: Greenvale Province, Thomson Orogen. |431+\-7 Ma|||||
25715|Dido Tonalite|73425|6|Mentioned|p16|Silurian|Silurian|Greenvale Province, Thomson Orogen.||||||
38879|Diglum Granodiorite|23799|5|Briefly described|p117|||Of Murray and others (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
38879|Diglum Granodiorite|24489|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38879|Diglum Granodiorite|24615|5|Briefly described|CD|Triassic|Triassic|[Rgdi/g].  Pinkish grey medium-grained biotite-hornblende granodiorite and granophyric groundmass.||||||
38879|Diglum Granodiorite|68008|3|Fully described|p334, p338, p428-429, p631-633|Late Triassic|Late Triassic|Previously mapped as an unnamed intrusion of Triassic tonalite (Dear et al., 1971). A NE-trending oval body 13 x 6km, located 30km SSW of Calliope. Named after Diglum Creek; forms low topography adjacent to it and its tributaries. Geophysics described and modelled. Geochemistry described. K-Ar dating is Late Triassic (Webb and McDougall, 1968; Muggeridge, 1973). Associated with disseminated Cu and Mo mineralisation, eg Booreco Creek prospect.||||Intrudes Mount Alma Formation and Rockhampton Group.|The central core is a pinkish-grey, medium-grained biotite-hornblende granodiorite; surrounded by a rim of biotite-hornblende quartz diorite to augite-hornblende-biotite tonalite. Local hornblende-augite gabbro.|
38879|Diglum Granodiorite|68679|5|Briefly described|p427-428, p431|Late Triassic|Late Triassic|Forms a small, oval body. Geochemistry briefly described. Other similar ages given.|221 Ma (K-Ar biotite: Webb and McDougall, 1968).||||A core of medium-grained granodiorite with a granophyric groundmass, and a rim of biotite-hornblende quartz diorite to augite-hornblende tonalite. Drilling reveals an unexposed hornblende-augite gabbro in the far NE of the pluton.|
38879|Diglum Granodiorite|73450|6|Mentioned|p11|||||||||
28100|Dinah Formation|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
28100|Dinah Formation|22781|4|Described|p18|Proterozoic|Proterozoic|Holroyd Group||||||
28100|Dinah Formation|23420|5|Briefly described|p 143 table 4.4|||Olders unit in the Holroyd Group. Thickness >500m||||||
28100|Dinah Formation|43596|4|Described|p17-18, p19 Tb. 1||Proterozoic|Of the Holroyd Group. Conformably overlain by Sugarbag Creek Quartzite. Max. thickness: 500m. Comprises three variants of slate, schist and gneissic rocks.||||||27-JAN-09
28100|Dinah Formation|43738|6|Mentioned|p48|||||||||
28100|Dinah Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||24-JAN-05
28100|Dinah Formation|69591|5|Briefly described|p79 Tb.2.6|||Savannah Province, Coen Inlier. >500m thick; base not exposed. Exposed in anticline cores. Forms elongate, folded and faulted bands south of Edward River.||Basal Holroyd Group.||Partly correlates with Olkolo Formation.|Slate, quartzite, schist and gneiss.|
70393|Dingle Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Pink, medium-grained, uneven-grained to slightly porphyritic biotite monzogranite.|
70393|Dingle Granite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Biotite monzogranite.|
35545|Dingo Diorite|23162|5|Briefly described|p881||Late Permian|Age: K-Ar hornblende age of 260Ma.||||||
35545|Dingo Diorite|68679|5|Briefly described|p361, p364|Permian|Permian|Northern Connors Subprovince. Early Permian. Age is approximate as only 8 analyses done due to low zircon yield.|286 +/- 7 Ma (U-Pb SHRIMP: Cross et al. 2012).|||||
35545|Dingo Diorite|68901|5|Briefly described|p2, p4, p61-63, p145|Triassic|Permian|northern New England Orogen, Bowen Region. SHRIMP results and analysis discussed in detail. Only 9 zircons analysed. Additional geochronology should be undertaken on this unit.|~286  Ma reconnaissance age|||Closely associated with  Early Triassic Gloucester Granite.|Dark-grey, fine-grained, even-grained diorite consisting mainly of plagioclase laths and subordinate euhedral-subhedral clinopyroxene grains.|15-NOV-18
35545|Dingo Diorite|69952|6|Mentioned|p85|Triassic|Permian|New England Orogen. Under 'Triassic heading but age given as early Permian?|286 +7.3/-7.2|||||28-SEP-18
35545|Dingo Diorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|286 Ma (crystallisation: U-Pb zircon SHRIMP)||||Diorite.|
36428|Dingo Mountain Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p28. K-Ar 299 +/- 9 Ma. Faulted against Glen Gordon Volcanics. Kennedy Province.||||||
36428|Dingo Mountain Granodiorite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36428|Dingo Mountain Granodiorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
79434|Dingo Prospect Skarn|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event||Williams Supersuite|||Massive actinolite-garnet endoskarn?|
79434|Dingo Prospect Skarn|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Maramungee Suite.|||Massive actinolite-garnet endoskarn?|
79434|Dingo Prospect Skarn|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Maramungee Suite.|||Massive actinolite-garnet endoskarn?
|
79434|Dingo Prospect Skarn|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Maramungee Suite|||Massive actinolite-garnet endoskarn?
|
79434|Dingo Prospect Skarn|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Maramungee Suite|||Massive actinolite-garnet endoskarn?
|
30727|Dipvale Granodiorite|23458|2|Defined|p115, p129|Mesoproterozoic|Mesoproterozoic|Age: 1746+/-7Ma. Southern foliated portion of the Capsize granodiorite now referred to as Dipvale Granodiorite. Intruded Corella Formation to south and Soldiers Gap Group to north. Major phase consists of medium-grained granodiorite to monzogranite.||||||27-AUG-07
30727|Dipvale Granodiorite|24256|6|Mentioned|p50 Fig.2|||Geological Province: Mount Isa Block.||||||
30727|Dipvale Granodiorite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
30727|Dipvale Granodiorite|50332|5|Briefly described|p20|Proterozoic|Proterozoic|Of the William and Naraku Batholiths. Age: 1760-1720Ma, (as in the Wonga Suite). Deformed biotite-muscovite pluton.||||||07-FEB-11
30727|Dipvale Granodiorite|65396|6|Mentioned|p53, p175|||||||||
30727|Dipvale Granodiorite|65505|6|Mentioned|980|Proterozoic|Proterozoic|Age: 1746 +/-7 Ma (U-Pb zircon).||||||
30727|Dipvale Granodiorite|66913|5|Briefly described|p171 fig 2|Statharian|Statherian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2.||||||
30727|Dipvale Granodiorite|67323|4|Described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Williams Igneous Event. See also reference to Dipvale Granite (p17-18, p24).|1746 +/- 7 Ma.|Wonga Suite.||Intrudes Corella Formation.|Medium-grained, hornblende-biotite granodiorite to monzogranite; pervasively foliated|
30727|Dipvale Granodiorite|69056|4|Described|p3, p14 Tb.3, p18, p23, p28, p46, p53|Statherian|Statherian|See also p57, Time-Space plot sheet. Wonga Event-aged granodiorite in Mary Kathleen Domain. Stated to have been previously called the Capsize Creek Complex. Modelling values listed. Hosts the Gem Cu-Au-Fe oxide deposit. Has a poorly-defined contact with the Mavis Granodiorite.|1746 +/- 7 Ma (Davis et al., 2001).|Wonga Suite.||Intrudes Corella Formation.|Pervasively foliated medium-grained hornblende-biotite granodiorite to monzodiorite.|
30727|Dipvale Granodiorite|69591|5|Briefly described|p36, p60|||Wonga Batholith, Mary Kathleen Domain, Mount Isa Province. An age of 1746 +/- 7 Ma by Davis et al. (2001) is also given.|1752 +/- 8 Ma (Pollard & McNaughton, 1997).||||Medium-grained, foliated hornblende-biotite granodiorite to monzogranite.|
30727|Dipvale Granodiorite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Medium-grained, hornblende-biotite granodiorite to monzogranite; pervasively foliated.|
30727|Dipvale Granodiorite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Medium grained, hornblende biotite granodiorite to monzogranite; pervasively foliated.|
30727|Dipvale Granodiorite|71592|5|Briefly described|Appendix A.|||Mary Kathleen Domain, Mount Isa Orogen.|1746+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
30727|Dipvale Granodiorite|72596|6|Mentioned|p24|Statherian|Statherian|Geochronologic constraint from Davis et al. (2001). Previously[?] Mavis Granodiorite.|1746 +/- 7 Ma|||||
30727|Dipvale Granodiorite|73413|6|Mentioned|p8, App.1|Statherian|Statherian|U-Pb SHRIMP age of 1746 +/- 7 Ma and a metamorphic age of 1505 +/- 7 Ma were reported by Davis et al. (2001).|1746 +/- 7 Ma||||Includes granodiorite.|
30727|Dipvale Granodiorite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Mary Kathleen Domain.|1746+/-7 Ma crystallisation age||||Felsic intrusive.|
30727|Dipvale Granodiorite|73553|4|Described|p4, p8 Fig.1.2.3, p102-107, p210-213|Statherian|Statherian|Mary Kathleen Domain, northeast part. Wonga Igneous Subprovince. Outcrops sporadically. Initially mapped as Naraku Granite (Carter et al., 1961), two subunits ('1' and '2') later mapped and described (Wilson et al., 1980). Informally referred to as Capsize granodiorite (Wyborn, 1998). Formally defined by Davis et al., (2001). Convoluted and uncertain boundary with Mavis Granodiorite. Intruded by thin dolerite and leucogranite/pegmatite bodies which are in turn cut by the Mavis Granodiorite. Assumed to be intruded by Mavis Granodiorite. Yellow to green/blue tones on radiometric images, aeromagnetic images show magnetic striping. Suggested that only one intrusive unit is present based on lithological, geophysical, structural and geochemical similarity with Mavis Granodiorite.|1746+/-7 Ma zircon U-Pb SHRIMP|||Intercalated with Mavis Granodiorite, intrudes Corella Formation|Medium-grained granodiorite to monzogranite. Xenoliths of contry rock occur in sheeted contact zone. Minor leucocratic and pegmatitic phases. All phases contain a pervasive, steeply dipping foliation.|
28260|Dirie Sandstone|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Inorunie Group.||||||02-JUL-04
28260|Dirie Sandstone|23291|4|Described|p83 Tb. 3.6|Early Paleozoic|Mesoproterozoic|Parent: Inorunie Group. Thickness: 350m? Geological Province: Georgetown Region.||||||30-JUN-15
28260|Dirie Sandstone|23510|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|of Inorunie Group.||||||
28260|Dirie Sandstone|40218|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
28260|Dirie Sandstone|40954|6|Mentioned|p132|||||||||
28260|Dirie Sandstone|41975|6|Mentioned|Fig.3 P433|||||||||
28260|Dirie Sandstone|43664|6|Mentioned|Fig.3,p15|||||||||
28260|Dirie Sandstone|68355|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Is overlain conformably by Chulcee Formation.|White to pale pink, massive fine- to coarse-grained orthoquartzite, rare micaceous (muscovite) quartzose sandstone.|
28260|Dirie Sandstone|68356|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Is overlain conformably by Chulcee Formation.|White to pale pink, massive fine- to coarse-grained orthoquartzite, rare micaceous (muscovite) quartzose sandstone.|
28260|Dirie Sandstone|69591|5|Briefly described|p75|||Croydon Province, Georgetown Inlier.||Inorunie Group.||||
36256|Disaster Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36256|Disaster Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36256|Disaster Granite|60425|4|Described|p284-5 Appdx.|||Of Nettle Suite (O'Briens Creek Supersuite). Included in Black Prince Granite together with Brownville, Glenlinedale, Stingo and Wilderness Granites on most recent maps. Fine-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
28042|Dixie Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes the Holroyd Group||||||
28042|Dixie Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p35|||Of Ebagoola Suite (Kintore Supersuite). Intrudes Dinah Formation and Sugrabag Creek Quartzite. White to pale buff, coarse, very uneven-grained to seriate or weakly porphyritic biotite-garnet-muscovite leucogranite.||||||27-JAN-09
28042|Dixie Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
41255|Dogherty Granite|50597|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Coarse grained biotite leucogranite.||||||30-JUN-04
41255|Dogherty Granite|50598|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Coarse grained biotite leucogranite.||||||
41255|Dogherty Granite|65388|3|Fully described|p247-248, p236 Fig. 81, p243|Late Carboniferous|Late Carboniferous|Southern Auburn Arch. In contact with the Evandale Tonalite, Flat Range Granodiorite and Ah Fat Granodiorite Complex, but relationship not known. Several masses separated by Glisson Granodiorite. Probably intrudes the Torsdale Volcanics to the west. Unconformably overlain by Evergreen Formation. Age assumed similar to Evandale Tonalite. Previously included in Kilbeggan Adamellite. Due to weathering and poor outcrop, mainly mapped from geophysical response. Main rock type uncertain. ||||||
41255|Dogherty Granite|68679|5|Briefly described|p404, p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Relationships with surrounding units unknown; irregular, poorly defined margins.||||Intrudes Torsdale Volcanics (probably).|Pink medium- to coarse-grained, porphyritic, leucocratic biotite syenogranite; grey fine- to medium-grained hornblende-biotite granodiorite; pink to grey, fine- to medium-grained, slightly porphyritic biotite granite or granodiorite.|
24924|Donaldsons Well Volcanic Member|23032|5|Briefly described|p12|Ordovician|Ordovician|||||||
24924|Donaldsons Well Volcanic Member|23424|5|Briefly described|p332|||Lower sequence of Judea Formation. Intruded by Saddington Tonalite. Graveyard Creek Subprovince.||||||
24924|Donaldsons Well Volcanic Member|23430|5|Briefly described|p476|||Of Judea Formation. Broken River Province.||||||
24924|Donaldsons Well Volcanic Member|23431|5|Briefly described|p541|||Of Judea Formation.||||||
24924|Donaldsons Well Volcanic Member|41260|3|Fully described|p29|||Reserved as Donaldsons Well Volcanics.||||||11-APR-07
24924|Donaldsons Well Volcanic Member|41679|6|Mentioned|Fig.2|||||||||
24924|Donaldsons Well Volcanic Member|41719|2|Defined|p215|Early Ordovician||||||||
24924|Donaldsons Well Volcanic Member|41739|6|Mentioned|Fig.2|||||||||
24924|Donaldsons Well Volcanic Member|41740|6|Mentioned|p222|||||||||
24924|Donaldsons Well Volcanic Member|42054|6|Mentioned|p273|||||||||
24924|Donaldsons Well Volcanic Member|42279|5|Briefly described|p27|||||||||
24924|Donaldsons Well Volcanic Member|42693|5|Briefly described|map legend|Ordovician||||||||
24924|Donaldsons Well Volcanic Member|42933|4|Described|p50|||of Judea Formation||||||
24924|Donaldsons Well Volcanic Member|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Judea Formation||||||
24924|Donaldsons Well Volcanic Member|68336|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.||Unit in Judea Formation.|||Altered aphyric basalt (locally pillowed); keratophyre (Na-rich rhyolite or dacite).|
24924|Donaldsons Well Volcanic Member|68341|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.||Unit in Judea Formation.|||Altered aphyric basalt (locally pillowed); keratophyre (Na-rich rhyolite or dacite).|
24924|Donaldsons Well Volcanic Member|68478|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.||Of the Judea Formation.|||Altered aphyric basalt (locally pillowed); keratophyre (Na-rich rhyolite or dacite).|
24924|Donaldsons Well Volcanic Member|68479|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.||Of the Judea Formation.|||Altered aphyric basalt (locally pillowed); keratophyre (Na-rich rhyolite or dacite).|
24924|Donaldsons Well Volcanic Member|69592|5|Briefly described|p253-255|Early Ordovician|Early Ordovician|Withnall (1989, 1993). Graveyard Creek Subprovince. Lack of vesiculation and fragmental rocks indicate deep-marine eruption. Geochemical plots.||Judea Formation.||Overlies Gray Creek Complex. Is intruded by Saddington and Netherwood Tonalites.|Mainly aphyric (rarely plagioclase-phyric) lava ranging from basalt to Na-rich rhyolite or keratophyre; typically massive, local pillow structures. Lenses of red jasper, locally manganiferous; local volcaniclastic sandstone and conglomerate.|
41251|Donore Granite Gneiss|50598|5|Briefly described|Map Legend|Carboniferous|Devonian|Biotite orthogneiss, aplite, microgranite, pegmatite dykes and veins.||||||21-JUL-04
41251|Donore Granite Gneiss|61087|5|Briefly described|Map Legend|Carboniferous|Devonian|Medium to coarse-grained, banded, locally migmatic, biotite orthogneiss; aplite, microgranite and pegmatite dykes and veins; dark grey, strongly elongated, fine-grained microdiorite xenoliths.||||||
41251|Donore Granite Gneiss|65388|3|Fully described|p235-238, p280, 236, 239, 240, 242|Early Carboniferous|Early Carboniferous|New name. Rawbelle Batholith, Auburn Province. Age: SHRIMP U-Pb zircon 345.5+/- 4.0 Ma, 349+/-6 Ma. K-Ar Middle Triassic ages from Whitaker & others (1974), are probably reset. Distinctive geochemistry. S-type granites. Variably foliated, fine to medium-grained, equigranular biotite granite grading into orthogneiss and intermixed with more migmatitic gneiss that may include paragneiss. Dykes and veins of aplite, microgranite and pegmatite are also common. Relationships with other units not clear. See also p247, 303, 304, 340, 432, 446.||||||
41251|Donore Granite Gneiss|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Auburn Subprovince. This unit, as well as the Mount Clairvoyant Granite, Carinya Granite and Horse Granite Gneiss, are all mapped under the same symbol, Cga.||||||
41251|Donore Granite Gneiss|68679|5|Briefly described|p312, p353, p404-406, p415|Carboniferous|Carboniferous|Northern New England Orogen. The oldest intrusive in the Auburn Subprovince.|342 +/- 4.0 Ma (SHRIMP: Fanning et al., 2009).||||S-type. Medium- to coarse-grained, banded, locally migmatitic biotite orthogneiss; aplite, microgranite and pegmatite dykes and veins; microdiorite xenoliths. Variably foliated.|
41251|Donore Granite Gneiss|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|343+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granitic gneiss.|
27981|Doolan Creek Rhyolite|23291|5|Briefly described|p38|||Parent: Featherbed Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
27981|Doolan Creek Rhyolite|23422|5|Briefly described|Plate 7.3|Late Carboniferous|Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|23423|4|Described|p307 Table 7.3||Late Carboniferous|Intruded by Ruddygore Granodiorite and Belgravia Granite. Featherbed Volcanic Group.||||||
27981|Doolan Creek Rhyolite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Featherbed Volcanic Group, Kennedy Province.||||||
27981|Doolan Creek Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Featherbed Volcanic Group.||||||
27981|Doolan Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V115. I-Type.||||||
27981|Doolan Creek Rhyolite|23616|5|Briefly described|Table 3 p52||Late Carboniferous|Unconformably overlies Hodgkinson Fm rocks; intruded by Ruddygore Granodiorite and Bungabilly Granite, as well as by dykes and pods of rhyolite and 'diorite'. Of Featherbed Volcanic Gp. O'lying unit Jamtin Rhyolite (c). Thick: ~200 m.||||||02-APR-15
27981|Doolan Creek Rhyolite|23713|5|Briefly described|p24 Fig 6||Late Carboniferous|I-type. Of Featherbed Volcanic Group.||||||
27981|Doolan Creek Rhyolite|24485|4|Described|p43 Tb.7|Late Carboniferous|Late Carboniferous|Underlying Unit: Hodgkinson Formation (unconformable). Parent: Featherbed Volcanic Group. Max Thickness: ~200m?||||||
27981|Doolan Creek Rhyolite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group.  Geological Province: Kennedy Province.||||||
27981|Doolan Creek Rhyolite|43083|5|Briefly described|p91|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Associated with the Doolan Creek Ring Complex.  recrystallised rhyolitic and rhyodacitic ignimbrite.||||||17-JUN-09
27981|Doolan Creek Rhyolite|43087|6|Mentioned|p83|||||||||
27981|Doolan Creek Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Dark-grey to greenish-grey, welded, strongly recrystallised lithic-poor ignimbrite.||||||15-JUN-06
27981|Doolan Creek Rhyolite|43254|5|Briefly described|map legend||Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|43259|4|Described|Appendix 1,p12.||Late Carboniferous|of Featherbed Volcanic Group.||||||
27981|Doolan Creek Rhyolite|43285|5|Briefly described|Map Legend||Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|43567|6|Mentioned|Fig.2,p398||Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|43625|6|Mentioned|p35|||||||||
27981|Doolan Creek Rhyolite|43626|1|Redefined|p36||Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27981|Doolan Creek Rhyolite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||31-MAY-04
27981|Doolan Creek Rhyolite|60425|3|Fully described|p48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Unconformable on Hodgkinson Fm. Intruded by Ruddygore Granodiorite and Bungabilly Granite. Thickness: ~200m?||||||07-FEB-11
27981|Doolan Creek Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Featherbed Volcanic Group.|||Medium to dark greenish-grey, or grey, welded, moderately crystal-rich to crystal-rich, lithics-poor, hornblende-biotite rhyodacitic to rhyolitic ignimbrite; extensively recrystallised.|
33137|Dooloo Tops Volcanics|24488|5|Briefly described|Map Legend|Triassic|Triassic|||||||
33137|Dooloo Tops Volcanics|24615|5|Briefly described|CD|Triassic|Triassic|[Rvd].  Rhyolitic ignimbrite, rhyolite, volcanic breccia.||||||
33137|Dooloo Tops Volcanics|61730|6|Mentioned|p1013|||Mapped by Bryan et al (2001). Probably now incorporated into the Lochenbar suite units?||||||
33137|Dooloo Tops Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
33137|Dooloo Tops Volcanics|68008|2|Defined|p209, p211-214, p397, p400-401,p439,p635|Triassic|Triassic|Defined in this study. Named after the plateau of Dooloo Tops. Mapped as part of Muncon Volcanics by Dear et al. (1971). Forms a 10 x 4 km belt along the crest of Dawes Range. The type section is along Warrong Creek, from the base of the unit to a waterfall at GR31560E 72789N. Subaerial eruptions. c.200m thick. No fossils or age-dating; Triassic age from similarities with other volcanic sequences. Possible age-equivalent to Winterbourne Volcanics.||||Overlies Three Moon Conglomerate and Rockhampton Group unconformably, and Monal Granodiorite nonconformably. Intrudes Monal Granodiorite.  Is (assumed to be) intruded by Warrong Teschenite.|Mainly rhyolitic ignimbrite; volcanic breccia and conglomerate are also widespread; also flow-banded rhyolite (lavas and dykes), basalt at the top of the sequence, rhyolite dyke swarms.|
33137|Dooloo Tops Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
33137|Dooloo Tops Volcanics|68679|5|Briefly described|p312-313, p338, p432, p434, p442-444|Late Triassic|Late Triassic|High plateaus at Dooloo Tops, northern New England Orogen. Similar to Winterbourne Volcanics.||||Overlies Monal Granodiorite.|Basaltic to andesitic lavas in lower parts, and rhyolite lavas, autoclastic breccias and intensely welded ignimbrites in upper parts. Swarms of closely spaced vertical rhyolite dykes, 1-5m wide, extend N and S.|
33137|Dooloo Tops Volcanics|73450|4|Described|p11-12|Norian|Carnian|Forms the topographic high plateau of Kroombit Tops and Dooloo Tops. Ignimbrites are locally columnar-jointed and intensely welded to rheomorphic (lava-like) indicating high temperature and/or low viscosity compositions. Include swarms of closely spaced vertical rhyolitic dykes. Yielded a U-Pb SHRIMP zircon age of 227.3 +/- 1.4 Ma from a dacitic ignimbrite (Cross et al., 2012).|227.3 +/- 1.4 Ma U-Pb SHRIMP||||Includes a lower eruption sequence dominated by basaltic to andesitic lavas and pyroclastic deposits and an upper sequence dominated by rhyolitic lavas, ignimbrites, breccias and tuffs.|
40572|Doom Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Dungaminnie Formation.|||
40572|Doom Supersequence|63114|5|Briefly described|p1253 Fig.2, p1260.|||Isa superbasin.|||Includes the Lawn Hill Formation|||
40572|Doom Supersequence|63866|5|Briefly described|p53-p54|Calymmian|Calymmian|Isa Superbasin.|c. 1585 Ma||Includes the Dungaminine Formation|||
40572|Doom Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Calymmian|Calymmian|Lawn Hill Platform. Shallow water environments.|Max. age c.1580 Ma.|||Is overlain ?unconformably by Roper Group.|Feldspathic siliciclastics, coarsening upward.|
40572|Doom Supersequence|65337|6|Mentioned|p34.|||No evidence of this in the MOUNT DRUMMOND area.||||||
40572|Doom Supersequence|66843|5|Briefly described|p38 Fig.10, p39|||Said to be "informally" named. Depositional cycles and lithofacies described.||||||
40572|Doom Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40572|Doom Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Isa Superbasin. Of Nathan Group, NT (p9). Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Camooweal - Murphy Domain, Mount Isa Inlier.|~1590-1575 Ma.|?Fickling Group||Overlies Wide Supersequence.|Brown and green shale, thin bedded siltstone and fine sandstone|
40572|Doom Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes the Lawn Hill Formation.||||||
40572|Doom Supersequence|69591|5|Briefly described|p27, p43, p47|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the upper part of the Lawn Hill Formation.||||Overlies Wide Supersequence. Is equated with upper part of Doomadgee Formation.||
40572|Doom Supersequence|70897|5|Briefly described|p39-40, Fig.1.7.2-4|||Maintains relatively tabular architecture throughout deposition. Age inferred from dating of detrital zircons in Constance Formation, South Nicholson Group.|1591 +/- 10 Ma.|||Overlies Wide Supersequence.||28-NOV-17
40572|Doom Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation.||||||
40572|Doom Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||||Brown and Green shale and flaggy, thin-bedded siltstone and fine-grained sandstone.|
40572|Doom Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Mesoproterozoic|Paleoproterozic|Both Gun and Doom Supersequences are the subject of further investigation for their Oil or Condensate potential.||||Overlies Wide Supersequence.||
40572|Doom Supersequence|73144|4|Described|p: 8-9, 12-13, 19-20, 23, 25, 40, 42-43|Calymmian|Calymmian|Sequence Stratigraphy. Isa Superbasin. Contains five third order sequences [see article for more detail on third order sequences]. Deposited via prograding wedge and fan, mid-shelf turbidites or mid-inner shelf (Krassay et al., 2000). Poorly preserved in [some] areas due to truncation at the base of the South Nicholson Group. Contemporaneous deposition with the Doom Event, at ~1575 Ma associated with north-south compression.|1575-1585 Ma|||Includes a portion of the Lawn Hill Formation.|Feldspathic and lithic sandstone, carbonaceous siltstone, dolostone, shale, carbonaceous/silty shale, black mudstone and black limestone.|
36410|Dora Granite|23424|5|Briefly described|p339|||S-Type.||||||
36410|Dora Granite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|S-Type. Also see p25-26. Kennedy Province.||||||
36410|Dora Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36410|Dora Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Muscovite-biotite granite.|
36410|Dora Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Muscovite-biotite granite.|
36410|Dora Granite|69030|5|Briefly described|p6|Permian|Permian|Clarke River Basin, Broken River Province.|||||S-type granitoids.|
36410|Dora Granite|69593|5|Briefly described|p492, p494, p496-497|||Kangaroo Hills Subprovince, Kennedy Igneous Association. Outcrop area ~15 km2. Age range probably Early to Mid- Carboniferous to Permian(?).|||||S-type. Tourmaline-bearing muscovite-biotite granite; distinctive quartz-tourmaline nodules up to ~15cm.|
69123|Doraville Granodiorite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Fine- to medium-grained, equigranular biotite granodiorite; intruded by andesite dykes; most outcrops strongly decomposed. Part of the Urannah Batholith.||||||16-MAR-06
69123|Doraville Granodiorite|65388|2|Defined|p363-365, p135 Fig. 53, p362, 373|Early Permian|Late Carboniferous|Northern Connors Arch, Southern Urannah Batholith. Connors Province. Extent from geophysics. Appears to intrude the Mia Mia Igneous Complex. Likely age given. Light grey, fine to medium-grained hornblende-biotite granodiorite. Most exposures very weathered.||||||
35134|Doreen Granite|23042|5|Briefly described|p73,4, Fig 2||Carboniferous|Intrudes Connors Volcanics.||||||
35134|Doreen Granite|60475|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Pinkish grey, equigranular, medium-grained, hornblende biotite granite to monzonite intruded by numerous fine grained felsic and andesitic dykes.||||||
35134|Doreen Granite|61035|4|Described|p9 Tb. 1|Early Permian|Late Carboniferous|Intrudes Leura Volcanics. Age: 300+/-4Ma (M. Fanning, SHRIMP). Geological Province: Connors Subprovince. Consists of equigranular, medium-grained, hornblende biotite granite to monzonite.||||||04-SEP-14
35134|Doreen Granite|65388|2|Defined|p366-367, p90 Fig. 37, p110|Early Permian|Late Carboniferous|Connors Arch pluton. Distribution extended to include an area formerly mapped as Connors Volcanics and the Iron Pot Granite. Intruded by andesite dyke swarm.  Intrudes Leura Volcanics. SHRIMP age: 301+/-3.4 Ma but may include inherited zircon, since appears to have hornfelsed 292+/-4 Ma Leura Volcanics? Equigranular pinkish grey, medium-grained, hornblende biotite granite to quartz monzonite.||||||
35134|Doreen Granite|68679|5|Briefly described|p357, p362|Permian|Pennsylvanian|Southern Connors Subprovince. This age determination is problematic as it is older than the Leura Volcanics which this Granite is interpreted to intrude.|300.9 +/- 3.4 Ma (SHRIMP: Fanning et al., 2009).|||Intrudes Leura Volcanics.||
35134|Doreen Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Quartz monzonite.|
41585|Dormans Flat Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Pale pinkish grey to pale reddish brown, fine-grained, highly porphyritic (allanite-titanite-hornblende-) biotite monzogranite.||||||
41585|Dormans Flat Granite|63748|4|Described|p44|||Previously mapped as Dundee Rhyodacite and Wallangarra Volcanics. Intrudes Wallangarra Volcs. Pale pinkish grey to reddish brown (iron-stained) fine-gr.(groundmass), highly porph. (allanite-titanite-hornblende-) biotite monzogranite. See also p27 Fig.27.||||||07-FEB-11
41585|Dormans Flat Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Sailor Jack and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
41585|Dormans Flat Granite|68679|5|Briefly described|p453, p455, p457-459|Early Triassic|Permian|Northern New England Batholith. ~11 km2. Is similar chemically, but not mineralogically or texturally, to the Sailor Jack Granite. Photographs, geochemical plot.||Sailor Jack Suite.||Intrudes the Wallangarra Volcanics.|Pink, pinkish grey to reddish brown, fine-grained, moderately to highly porphyritic biotite quartz monzonite to monzogranite; accessory hornblende, titanite, allanite; local well-developed quench texture. Oxidised, moderately evolved, high-K, I-type.|
41585|Dormans Flat Granite|68901|6|Mentioned|p68 Fig. iii|Early Triassic|Late Permian|||||||26-SEP-18
41585|Dormans Flat Granite|69639|6|Mentioned|p220|||||||||
41585|Dormans Flat Granite|71628|6|Mentioned|p12: 6|||Donchak et al. (2007) after unpublished work by Purdy (2003). See Dormans Flat Monzogranite.||||||
82410|Dormans Flat Monzogranite|71628|5|Briefly described|p12: 1-2, 6-8|||Donchak et al. (2007). First mapped by Purdy (2003; unpublished). Named after a local geographic feature. An irregular shaped intrusion of ~11 km2, ~7 km W of Wallangarra. Geochemistry described.||Dormans Flat Suite.||Intrudes Wallangarra Volcanics.|Pale pinkish grey to pale reddish brown, fine-grained, highly porphyritic biotite-(hornblende) monzogranite. I-type.|
23555|Dosey Limestone|23032|5|Briefly described|p28 fig6|Devonian|Devonian|||||||
23555|Dosey Limestone|23424|5|Briefly described|Table 8.1 p336|Givetian|Emsian|Of Wando Vale Subgroup/Broken River Group, Graveyard Creek Subprovince.||||||
23555|Dosey Limestone|23522|5|Briefly described|p250 Fig 6|Givetian|Eifelian|||||||
23555|Dosey Limestone|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Givetian|Eifelian|Of the Broken River Group. Overlain by the Papilio Formation. Overlies the Dosey Limestone. Limestone is Ls in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
23555|Dosey Limestone|41260|3|Fully described|p69|||||||||
23555|Dosey Limestone|41679|2|Defined|p259|Givetian|Eifelian|||||||
23555|Dosey Limestone|41719|6|Mentioned|Fig.2|||||||||
23555|Dosey Limestone|41739|6|Mentioned|Fig.2|||||||||
23555|Dosey Limestone|41740|6|Mentioned|p222|||||||||
23555|Dosey Limestone|42015|6|Mentioned|p318|||||||||
23555|Dosey Limestone|42031|5|Briefly described|Fig.5 P762|||||||||
23555|Dosey Limestone|42032|6|Mentioned|p505|||See also Fig.12||||||
23555|Dosey Limestone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
23555|Dosey Limestone|42933|3|Fully described|Table 2|||See also p104||||||
23555|Dosey Limestone|50093|4|Described|p237, p329 Fig.2|Givetian|Eifelian|Conformably overlies Storm Hill Sandstone, overlain by Papilio Formation. Of Broken River Group.||||||21-JUN-13
23555|Dosey Limestone|63152|5|Briefly described|p120 Fig. 3|Givetian|Eifelian|Of the Broken River Group. Highly fossiliferous, lithologically diverse carbonate complex.||||||10-APR-07
23555|Dosey Limestone|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23555|Dosey Limestone|68336|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; lesser quartzose sandstone, calcareous sandstone and mudstone and impure sandy limestone.|
23555|Dosey Limestone|68341|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; lesser quartzose sandstone, calcareous sandstone and mudstone and impure sandy limestone.|
23555|Dosey Limestone|68478|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; lesser quartzose sandstone, calcareous sandstone and mudstone and impure sandy limestone.|
23555|Dosey Limestone|68479|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; lesser quartzose sandstone, calcareous sandstone and mudstone and impure sandy limestone.|
23555|Dosey Limestone|69079|6|Mentioned|p68|||||Broken River Group.||||
23555|Dosey Limestone|69592|5|Briefly described|p259, p264-266|Middle Devonian|Early Devonian|Southern Graveyard Creek Subprovince, Broken River Province. Up to 230m thick; thins northwards. The lower part is finer-grained in the type section, and contains abundant Amphipora debris. Shallow-marine carbonate shelf deposits. Late Eifelian to early Givetian.||Wandovale Subgroup.||Overlies Storm Hill Sandstone or, where absent, Lomandra Formation. Is overlain by Papillio Formation. Lateral equivalent of Burges Formation.|Bioclastic limestone, calcareous quartzose sandstone and siliciclastic mudstone. The carbonate rocks are heterogeneous, ranging from lime mudstone to calcirudite with wackestone, grainstone and packstone fabrics; local stromatoporoid boundstone.|
27391|Dotswood Group|22800|5|Briefly described|Fig.14 p592, p591|Famennian||||||||
27391|Dotswood Group|23422|4|Described|p180, p206 Table 6.3|Late Devonian|Late Devonian|Overlain by Keelbottom Group. Underlain by Fanning River Group. Maximum thickness: 2000m. Geological Province: Burdekin Basin.||||||13-NOV-07
27391|Dotswood Group|23430|5|Briefly described|p491|||Overlain by Keelbottom Group. Burdekin Basin Province.||||||23-APR-08
27391|Dotswood Group|23431|5|Briefly described|p538|||Burdekin Basin Province.||||||
27391|Dotswood Group|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27391|Dotswood Group|23522|5|Briefly described|p259|Late Devonian|Late Devonian|||||||
27391|Dotswood Group|23893|5|Briefly described|p16|Famennian|Frasnian|Geological Province: Burdekin Province.||||||
27391|Dotswood Group|24577|5|Briefly described|p755 Fig. 2|Devonian|Devonian|Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
27391|Dotswood Group|24610|5|Briefly described|p62|Late Devonian|Late Devonian|Unconformably underlain by Fanning River Group. Geological Province: Burdekin Basin.||||||19-FEB-07
27391|Dotswood Group|24612|5|Briefly described|p7|Late Devonian|Late Devonian|Underlain by Fanning River Group. Geological Province: Burdekin Basin.||||||23-APR-08
27391|Dotswood Group|24613|2|Defined|p3, p6 Fig. 6, p34|Late Devonian|Late Devonian|Comprises Vanneck, Stud and Julie Formations + proposed Kukiandra Fm. Unconform.on Fanning River Gp; conformable below Myrtlevale Fm. Max.thickness: 2550m. Geol.prov: Burdekin Basin. Sandstone, siltstone, mudstone, conglomerate - detailed lith. incl.||||||07-FEB-11
27391|Dotswood Group|24614|4|Described|p191 Fig. 1, p194-5|Frasnian|Frasnian|Includes Vanneck, Stud and Julia Formations - entirely non-marine. Gradationally and unconformably overlies the Fanning River Group; conformably overlain by Keelbottom Group. Geological Province: Burdekin Basin. See also p193 Fig. 2.||||||07-FEB-11
27391|Dotswood Group|31285|4|Described|p82|||Frasnian. Formations listed.||||||
27391|Dotswood Group|32865|4|Described|p478|||Late Dev.||||||
27391|Dotswood Group|37565|6|Mentioned|Fig.6|||||||||
27391|Dotswood Group|37573|4|Described|p210|||See also Figs.2,5,7||||||
27391|Dotswood Group|39445|6|Mentioned|p80|||See also Table 6||||||
27391|Dotswood Group|39686|4|Described|p78|||||||||
27391|Dotswood Group|39731|6|Mentioned|p31|||||||||
27391|Dotswood Group|39732|6|Mentioned|p29|||||||||
27391|Dotswood Group|39735|6|Mentioned|p18|||||||||
27391|Dotswood Group|40623|5|Briefly described|p88|||||||||
27391|Dotswood Group|41385|6|Mentioned|p363|||||||||
27391|Dotswood Group|41735|6|Mentioned|p284|||||||||
27391|Dotswood Group|41774|6|Mentioned|p31|||||||||
27391|Dotswood Group|42295|5|Briefly described|Fig.2 P5|||||||||
27391|Dotswood Group|42407|6|Mentioned|p22|||||||||
27391|Dotswood Group|42689|5|Briefly described|map legend|Late Devonian||||||||
27391|Dotswood Group|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27391|Dotswood Group|42692|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
27391|Dotswood Group|42750|6|Mentioned|p46|||||||||
27391|Dotswood Group|42933|5|Briefly described|p154|||||||||
27391|Dotswood Group|43095|5|Briefly described|Plate 2|||||||||
27391|Dotswood Group|43589|6|Mentioned|p25||Late Devonian|Intruded by Pall Mall Granite.||||||23-APR-08
27391|Dotswood Group|43933|5|Briefly described|Map Legend||Late Devonian|||||||
27391|Dotswood Group|43935|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27391|Dotswood Group|62522|2|Defined|p21|Frasnian|Frasnian|Includes: Vanneck, Stud, Julia and Kukiandra Formations. Unconformable on Fanning River Group; conformable/disconformable below Keelbottom Group. Max. thickness: 2550m. Geological Province: Burdekin Basin.||||||13-NOV-07
27391|Dotswood Group|63154|5|Briefly described|p285 Fig. 5|Devonian|Devonian|Geological province: Charters Towers Province. Mixed shallow marine sediments.||||||
27391|Dotswood Group|67402|5|Briefly described|p246|Famennian|Frasnian|Burdekin Basin. |||Includes the Vanneck Formation, Stud Formation, Julia Formation and the Kukiandra Formation.|Overlies the Fanning River Group. Overlain by the Keelbottom Group.||
27391|Dotswood Group|68350|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.|||Includes Vanneck, Stud and Julia Formations.|Conformably overlies Fanning River Group.|Undivided quartzose to feldspathic sandstone, polymictic conglomerate and red mudstone and siltstone.|
27391|Dotswood Group|68351|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.|||Includes Vanneck, Stud and Julia Formations.|Conformably overlies Fanning River Group.|Undivided quartzose to feldspathic sandstone, polymictic conglomerate and red mudstone and siltstone.|
27391|Dotswood Group|68419|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin.|||Includes Julia Formation, Stud Formation, and Vanneck Formation.|Conformably underlain by the Fanning River Group.|Feldspathic to quartzose sandstone, polymictic conglomerate, and red mudstone and siltstone.|
27391|Dotswood Group|68420|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin.|||Includes Julia Formation, Stud Formation, and Vanneck Formation.|Conformably underlain by the Fanning River Group.|Feldspathic to quartzose sandstone, polymictic conglomerate, and red mudstone and siltstone.|
27391|Dotswood Group|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Burdekin Basin.||||||
27391|Dotswood Group|68576|5|Briefly described|Q_11: p41|Late Devonian|Late Devonian|||||Is overlain probably unconformably by Nulla Basalt.|Redbeds.|
27391|Dotswood Group|68731|5|Briefly described|p183, p184, p185 Tb 3.4, p186 Fig 3.100|Late Devonian|Late Devonian|Burdekin Basin. Stratigraphic content and definition revised by Lang, Gunther and Rich (1990) and Lang and Draper (1995). Registers a range of fluviatile and sporadic lacustrine depositional environments.|||Includes Kukiandra Formation, Julia Formation, Stud Formation, and Vanneck Formation.||Siliciclastic, predominantly fluviatile, but thin, shallow-marine carbonates also occur.|03-JUL-14
27391|Dotswood Group|69592|5|Briefly described|p274 Fig.4.65, p276|Mississippian|Late Devonian|Burdekin Basin. Coeval with Bulgeri and Turrets Formations.||||||
30377|Double Barrel Andesite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Gingerella Cauldron Complex, Sundown Volcanic Group.||||||
30377|Double Barrel Andesite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Volcanic No. V90.||||||
30377|Double Barrel Andesite|23616|5|Briefly described|Table 3 p54||Late Carboniferous|Of Sundown Volcanic Group. Overlying unit Gingeralla Volcanics - conformable. Dargalong Province. Max. thickness ~45 m.||||||
30377|Double Barrel Andesite|43259|5|Briefly described|Appendix 1,p9|Permian|Carboniferous|Bultitude & Hutton 1992.||||||
30377|Double Barrel Andesite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
30377|Double Barrel Andesite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gingerella Cauldron Complex.|||Grey, porphyritic, andesitic and dacitic lava (locally autobrecciated), tuff and possible pyroclastic-flow deposits.|
30377|Double Barrel Andesite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Gingerella Cauldron Complex.|||Grey, porphyritic, andesitic and dacitic lava (locally autobrecciated), tuff and possible pyroclastic-flow deposits.|
24253|Double Crossing Metamorphics|22461|5|Briefly described|Fig 1 p464|||Of the Soldiers Cap Group?||||||25-JUN-09
24253|Double Crossing Metamorphics|22515|6|Mentioned|p397|Statherian||||||||
24253|Double Crossing Metamorphics|23064|6|Mentioned|136|||||||||
24253|Double Crossing Metamorphics|23068|5|Briefly described|p784 (fig 1)|||||||||
24253|Double Crossing Metamorphics|23069|5|Briefly described|p775 (fig 1)|||||||||
24253|Double Crossing Metamorphics|23333|5|Briefly described|1114 Fig.1|||||||||
24253|Double Crossing Metamorphics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1740+/-6Ma.||||||05-FEB-07
24253|Double Crossing Metamorphics|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
24253|Double Crossing Metamorphics|23973|5|Briefly described|p1436|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: >1875Ma.||||||
24253|Double Crossing Metamorphics|24254|5|Briefly described|p23|Proterozoic|Proterozoic|Max. Age: 1840 Ma (zircon). Geological Province: Mount Isa Inlier.||||||
24253|Double Crossing Metamorphics|37862|4|Described|p587|||||||||
24253|Double Crossing Metamorphics|38234|4|Described|p104|||||||||
24253|Double Crossing Metamorphics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24253|Double Crossing Metamorphics|38658|6|Mentioned|p152|||||||||
24253|Double Crossing Metamorphics|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||25-AUG-04
24253|Double Crossing Metamorphics|39445|5|Briefly described|Table 2|||||||||
24253|Double Crossing Metamorphics|39622|6|Mentioned|p19|||||||||
24253|Double Crossing Metamorphics|40840|6|Mentioned|Map legend|||||||||
24253|Double Crossing Metamorphics|41306|4|Described|p5|||||||||
24253|Double Crossing Metamorphics|41381|6|Mentioned|p325|||||||||
24253|Double Crossing Metamorphics|41978|4|Described|p493|||||||||
24253|Double Crossing Metamorphics|41979|6|Mentioned|Fig.2 P512|||||||||
24253|Double Crossing Metamorphics|42565|5|Briefly described|Table 1 P6, P3|||||||||
24253|Double Crossing Metamorphics|44195|5|Briefly described|p345 Table 1,349|||Actually spelt Double Crossing Mets. Maximum age: 1840 +/-20 Ma ( U-Pb).||||||05-FEB-07
24253|Double Crossing Metamorphics|45161|4|Described|p41|||||||||
24253|Double Crossing Metamorphics|45166|4|Described|p10|||||||||
24253|Double Crossing Metamorphics|49009|2|Defined|p13|Proterozoic|Proterozoic|Included as part of Williams Granite by Carter & Opik (1963).||||||
24253|Double Crossing Metamorphics|49041|5|Briefly described|Table 3|||||||||
24253|Double Crossing Metamorphics|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Deformed biotite-muscovite pluton body.  Geological Province: Eastern Fold Belt Province.||||||
24253|Double Crossing Metamorphics|50536|5|Briefly described|p6.1, 11.4|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1740 +/- 6Ma (Shrimp).||||||07-NOV-08
24253|Double Crossing Metamorphics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Gneiss, schist, amphibolite, quartzite.||||||
24253|Double Crossing Metamorphics|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||18-JUL-13
24253|Double Crossing Metamorphics|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
24253|Double Crossing Metamorphics|61929|5|Briefly described|p130 Fig. 4|||||||||
24253|Double Crossing Metamorphics|61933|5|Briefly described|p169 Fig.1|||See also p171 Tb.1.||||||12-MAY-06
24253|Double Crossing Metamorphics|61936|5|Briefly described|p190 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1745-1740Ma. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p195 Fig. 6. ||||||07-NOV-08
24253|Double Crossing Metamorphics|63866|5|Briefly described|p62, p70|Orosirian|Orosirian|Mitakoodi-Marimo-Stavely Zone. Outcrops west of the Selwyn mine.|1840 +/- 20 Ma (Page and Sun, 1998)||||Sillimanite feldspathic gneisses.|
24253|Double Crossing Metamorphics|64248|6|Mentioned|p33 Fig.1, p36, p38 Fig.5, p46|Orosirian|Orosirian|Metamorphosed at 1740 +/- 6 Ma. Appears in lower case on p36 and p46. Foster and Austin (2008) proposed replacing Double Crossing Metamorphics with Ballara/Mitakoodi Quartzites.|<1814 +/- 10 Ma (deposition).|||||11-DEC-17
24253|Double Crossing Metamorphics|64249|5|Briefly described|p83|Paleoproterozoic|Paleoproterozoic|Age range of deposition: 1762-1742Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
24253|Double Crossing Metamorphics|64250|5|Briefly described|p7, p9-12, p23|Statherian|Orosirian|Cloncurry Fold Belt, Mount Isa Inlier. Metamorphosed by Gin Creek Granite at 1740 +/- 6 Ma. Is no longer considered as basement.|<1814 +/- 10 Ma: deposition.|||Is overlain by Answer Slate and Staveley Formation.|Micaceous and feldspathic gneiss and schist, migmatitic gneiss; minor augen gneiss, amphibolite and quartzite.|12-MAY-14
24253|Double Crossing Metamorphics|65396|5|Briefly described|p7, p12, p43, p82, p84, p105, p169|Orosirian|Orosirian|See also p172-176, p180-182, p195-196, p202, p218, p229, p241, p437-438. Basement in Mount Isa Block. Cloncurry Fold Belt. Crops out to the east of Gin Creek Granite which metamorphosed the rocks to upper amphibolite facies (with local migmatisation). Might correlate with Tewinga Group and with Fullarton River Group. Cover Sequence 2. Is intruded by a felsic leucosome aged c.1740 Ma containing detrital zircons aged c.1814 Ma. Detrital zircon sources listed. Appears as Double Crossing metamorphics on p229.|<1814 +/- 10 Ma; >1740 +/- 6 Ma.|||Correlated with Argylla Formation, Mitakoodi Quartzite, Fullarton River Group. Conformably underlies Answer Slate and Staveley Formation (possible tectonic contact). Is intruded by Gin Creek Granite.|Micaceous and feldspathic gneiss and schist, migmatitic gneiss and minor augen gneiss, amphibolite and quartzite.|
24253|Double Crossing Metamorphics|66913|5|Briefly described|p170 fig 1||||1700-1725 Ma|||||
24253|Double Crossing Metamorphics|67323|5|Briefly described|p15, p18-19, p24, p39, p77, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Oldest rocks in the Marimo-Staveley Domain. Gneissic domes: probably metamorphic core complexes. Strong magnetic response. Could have formed during the Wonga Event. Maximum deposition ages by Carson et al. (in prep.) and Magee et al. (in prep.) respectively. Metamorphosed at ~1740 Ma from greenschist to upper amphibolite facies.|1752 +/- 4 Ma and 1743 +/- 17 Ma.|||Surrounds Gin Creek Granite and Houdini Granite. Is faulted against Answer Slate, Staveley Formation and Kuridala Formation. Age-equivalent to Marraba Volcanics.|Quartz-feldspar-mica gneiss, migmatitic gneiss and biotite schist adjacent to Gin Creek Granite; local quartzite, feldspathic quartzite and quartz-hematite rock; grade outwards into chlorite schist and metasiltstone; local amphibolite, metadolerite.|
24253|Double Crossing Metamorphics|67539|4|Described|p11, p14|Statherian|Orosirian|Contains a sharp contact with the Staveley Formation. Detrital zircons from this unit have yielded two ages: 1840 Ma and 1770 Ma.|~ 1840 Ma; 1770 Ma|||Intruded and contact metamorphosed by the Gin Creek Granite.|High-grade gneiss and migmatite through to metabasalt, biotite-rich schist and chlorite metasiltstone.|
24253|Double Crossing Metamorphics|68021|6|Mentioned|p137|||?Basement to Leichhardt Superbasin.||||||
24253|Double Crossing Metamorphics|68146|4|Described|p3, p6, p75-82, p200-202, p211|||Marino-Stavely Domain, 80km S of Cloncurry. Crops out in the core of two antiforms; poorly exposed as sparse, intermittent low "ribs" of exposed rock. Other ages, older and younger, are given and all age determinations discussed. This unit may be equivalent in age to the Marraba Volcanics in the adjacent Mitakoodi Block. Whole-rock Sm-Nd isotopic data tabulated.|1752 +/- 4 Ma maximum depositional age.|||Is structurally overlain by Staveley Formation and Answer Slate (detachment surface). Is intruded by Gin Creek Granite.|A heterogeneous, well-foliated fissile package of greenschist to upper-amphibolite facies psammites and pelites; comprises alternating sandy to pelitic beds on a decimetre scale.|
24253|Double Crossing Metamorphics|68542|6|Mentioned|p16 fig 4|||||||||
24253|Double Crossing Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
24253|Double Crossing Metamorphics|68575|4|Described|p2-3,p6-7,p44-52,p63-64,p125-126,p134|||Mount Isa Region. Sediments were probably deposited, metamorphosed and intruded in relatively rapid succession. Previously dated (MDA) at c.1840 Ma by Page and Sun (1998), but a more precise MDA of 1752 +/- 4 Ma is from Carson et al.(2011). Crosscutting leucosomes in migmatitic gneiss from this unit were dated at 1740 +/- 6 Ma (Page and Sun, 1998). May be age-equivalent to the Marraba Volcanics. Whole rock Sm-Nd isotopic data and age (1743 Ma).|1744 +/- 18 Ma (maximum deposition age).|||Is intruded by the Gin Creek Granite. Is faulted against Staveley Formation.|Dark grey metasiltstone interbedded with subordinate light brown, fine-grained meta-sandstone, progressing through chlorite schist into biotite schist, gneiss and migmatite, localised around Gin Creek Granite. Some metabasalt.|
24253|Double Crossing Metamorphics|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
24253|Double Crossing Metamorphics|69056|4|Described|p5, p54, Time-Space plot sheet|Statherian|Statherian|Marimo-Staveley Domain. Metamorphosed and intruded during the ~1740 Ma Wonga Event. Maximum depositional age. Other age determinations given.|1743 +/- 17 Ma (Magee et al., 2012).|||Envelops the Gin Creek Granite.|Low-grade chlorite schists to migmatitic gneisses.|
24253|Double Crossing Metamorphics|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Quartz-feldspar-mica gneiss, migmatitic gneiss and biotite schist adjacent to Gin Creek Granite; local quartzite, feldspathic quartzite and quartz-hematite rock; grade outwards into chlorite schist and metasiltstone; local amphibolite and metadiorite|
24253|Double Crossing Metamorphics|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Quartz-feldspar-mica gneiss, migmatitic gneiss and biotite schist adjacent to Gin Creek Granite; local quartzite, feldspathic quartzite and quartz-hematite rock; grade outwards into chlorite schist and metasiltstone;local amphibolite and metadiorite|
24253|Double Crossing Metamorphics|69591|5|Briefly described|p29, p33, p35-37, p57, p105|Paleoproterozoic|Paleoproterozoic|Oldest rocks in the Marimo-Staveley Domain, Leichhardt Superbasin, Mount Isa Province. Part of Myally Supersequence. Occurs in an antiformal structure (?metamorphic core complex). May correlate with Marraba Volcanics. Deformed in the ~1740 Ma Wonga Extension Event. Separated from the overlying Staveley Formation by an inferred folded decollement.|1752 +/- 4 Ma (MDA: Carson et al., 2011).|||Surrounds (?is intruded by) the Gin Creek Granite and Houdini Granite.|Quartz-feldspar-mica gneiss, migmatitic gneiss and biotite schist adjacent to Gin Creek Granite; local quartzite, feldspathic quartzite and quartz-hematite rock; grading out into chlorite schist and metasiltstone; local amphibolite and metadolerite.|
24253|Double Crossing Metamorphics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1752+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone.|
24253|Double Crossing Metamorphics|72889|5|Briefly described|p5, p6 Fig.i. p8, p27, p30.|Statherian|Statherian|Previous age determinations: 1740 +/- 6 Ma magmatic pegmatite formation age; Page and Sun, 1998; 1752 +/- 4 Ma maximum depositional age; Magee et al., 2012; Withnall, 2019.|1752 +/- 4 Ma|||Intruded by Gin Creek Granite.||
24253|Double Crossing Metamorphics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
24253|Double Crossing Metamorphics|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
24253|Double Crossing Metamorphics|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Kuridala-Selwyn-Marimo-Doherty Domain.|1752+/-4 Ma maximum depositional age||||Metamorphics, minor mafic extrusives.|
24253|Double Crossing Metamorphics|73529|5|Briefly described|p15 Fig.1, p17|||Also written as Double Crossing metamorphics.||||Intruded by Gin Creek Granite|Metasediments.|
74237|Dozer Creek Granite|69593|5|Briefly described|p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.||||I-type.|
28513|Drake Volcanics|22580|5|Briefly described|p97,p99||Late Permian|||||||
28513|Drake Volcanics|22857|4|Described|p258, p536 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Wandsworth Volcanic Group. Rhyodacitic to andesitic flows, crystal-lithic tuffs, breccias and agglomerates. Max. thickness: 1500m. Geological Province: New England Fold Belt. See also p319 Fig. 22.10B. ||||||
28513|Drake Volcanics|22864|6|Mentioned|p258|||||||||
28513|Drake Volcanics|22865|6|Mentioned|Fig22.10bp319|Early Triassic|Late Permian|||||||
28513|Drake Volcanics|23103|5|Briefly described|p551, Fig.1|Permian|Permian|||||||
28513|Drake Volcanics|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Parent: Wandsworth Volcanic Group.  Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Complexly interbedded rhyodacitic to andesitic flows, tuffs, breccias and volcanilithic sedimentary rocks.||||||12-DEC-07
28513|Drake Volcanics|23812|5|Briefly described|p28 Tb.3, p30|Late Permian|Early Permian|Of Wandsworth Volcanic Group. Intruded by Dumbudgery Creek Granodiorite and Bungulla Monzogranite. Maximum thickness:1500m.||||||
28513|Drake Volcanics|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|29988|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
28513|Drake Volcanics|30911|6|Mentioned|Map legend|Permian|Permian|||||||
28513|Drake Volcanics|31694|6|Mentioned|p350|||||||||
28513|Drake Volcanics|31993|6|Mentioned|p683|||||||||
28513|Drake Volcanics|32086|6|Mentioned|p325|||Subhorizontal andesitic volcanics||||||
28513|Drake Volcanics|32484|4|Described|p721|||||||||
28513|Drake Volcanics|32491|5|Briefly described|p14|||Permian||||||
28513|Drake Volcanics|32492|6|Mentioned|Map legend|Late Permian|Early Permian|Lower - Upper Permian||||||
28513|Drake Volcanics|32672|6|Mentioned|p675|||||||||
28513|Drake Volcanics|32880|6|Mentioned|p3|||L.-U.Perm.||||||
28513|Drake Volcanics|33005|6|Mentioned|p11|||See also P13||||||
28513|Drake Volcanics|33436|6|Mentioned|Table 1|||Perm. Refers Voisey (1958). Cheviot Hills Gp.||||||
28513|Drake Volcanics|33476|6|Mentioned|Table 1|||||||||
28513|Drake Volcanics|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
28513|Drake Volcanics|34340|6|Mentioned|Table 6.1|||Permian||||||
28513|Drake Volcanics|34556|5|Briefly described|p268|||Permian. Cheviot Hills Group||||||
28513|Drake Volcanics|35911|6|Mentioned|p60|||Discussion re mineral deposits.||||||
28513|Drake Volcanics|36936|6|Mentioned|p208|||||||||
28513|Drake Volcanics|36961|6|Mentioned|p212|||||||||
28513|Drake Volcanics|38806|6|Mentioned|p76|||Geological Province: New England Fold Belt||||||
28513|Drake Volcanics|38837|6|Mentioned|p234|||||||||
28513|Drake Volcanics|39279|3|Fully described|p367|||See also p370.||||||12-DEC-07
28513|Drake Volcanics|39282|6|Mentioned|p401|||Au/Ag mineralisation||||||
28513|Drake Volcanics|40245|6|Mentioned|p182|||Mention Table 1||||||
28513|Drake Volcanics|40504|6|Mentioned|p97|||||||||
28513|Drake Volcanics|40505|5|Briefly described|p81|||||||||
28513|Drake Volcanics|40506|6|Mentioned|p76|||||||||
28513|Drake Volcanics|40514|6|Mentioned|p7|||||||||
28513|Drake Volcanics|40773|3|Fully described|p458|||Mention p458.||||||12-DEC-07
28513|Drake Volcanics|41413|4|Described|p327|||||||||
28513|Drake Volcanics|41474|6|Mentioned|p62|||||||||
28513|Drake Volcanics|42378|5|Briefly described|Table 1 P10|||Andrews 1908||||||
28513|Drake Volcanics|42559|5|Briefly described|p10|||Correlated with Wallangarra Volcanics.||||||
28513|Drake Volcanics|42963|5|Briefly described|p5|||||||||
28513|Drake Volcanics|43017|5|Briefly described|Fig.2,p374|||||||||
28513|Drake Volcanics|43385|14|Not recorded|p179,180||Sakmarian|||||||
28513|Drake Volcanics|43881|14|Not recorded|p6-7,9|||Formation of Cheviot Hills Group||||||
28513|Drake Volcanics|44093|5|Briefly described|p233 App. 1|Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
28513|Drake Volcanics|44852|14|Not recorded|p60|Permian|Late Carboniferous|||||||
28513|Drake Volcanics|46525|6|Mentioned|p148|||||||||
28513|Drake Volcanics|48940|3|Fully described|p49|||||||||
28513|Drake Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
28513|Drake Volcanics|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|Of the Wandsworth Volcanic Group.||||||
28513|Drake Volcanics|60995|5|Briefly described|p51 Fig. 3|Early Triassic|Late Permian|Includes granite. Geological Province: Clarence-Moreton Basin. See also p56 Fig. 7.||||||
28513|Drake Volcanics|60996|6|Mentioned|p79|||Geological Province: Clarence-Moreton Basin.||||||
28513|Drake Volcanics|61772|6|Mentioned|p128, p133||Late Permian|In southern New England Orogen.||||||24-SEP-08
28513|Drake Volcanics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
28513|Drake Volcanics|61795|5|Briefly described|p368|Permian|Permian|Geological Province: New England Fold Belt. May be co-magmatic with Clarence River Supersuite.||||||17-NOV-08
28513|Drake Volcanics|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Andesite, dacite; minor rhyolite and associated pyroclastic rocks.||||||
28513|Drake Volcanics|63748|6|Mentioned|p20, p69|Late Permian|Late Permian|Correlated with Wallangarra Volcanics (Olgers et al 1974).||||||07-FEB-11
28513|Drake Volcanics|68111|5|Briefly described|p968 Tb.1, p970 Fig.2, p976|Capitanian|Wordian||264.4 +/- 2.5 Ma; U-Pb SHRIMP(Cross et al. 2010) |Of the Wandsworth Volcanic Group.||||
28513|Drake Volcanics|68679|6|Mentioned|p453|||Mentioned only as being older than the Emmaville Volcanics.||||||
28513|Drake Volcanics|69323|5|Briefly described|p1,70|Guadalupian|Guadalupian|Geological province: New England Orogen. Previosuly regarded as part of the basal succession of the Wandworth Volcanic Group, however has been dated at 264.4+\-2.5 Ma and its chemical composition is distinct from that of the Wandsworth Volcanic Group.|264.4+\-2.5 Ma (Cross and Blevin 2010)|||||
28513|Drake Volcanics|69639|5|Briefly described|p2, p182, p222|Guadalupian|Guadalupian|New England Orogen.|264.4 +/- 2.5 Ma; Cross and Blevin, 2010.|||Intruded by the Morgans Creek Monzogranite.||
28513|Drake Volcanics|69793|6|Mentioned|p1110, p1113 Fig.3|Permian|Permian|Southern New England Orogen.||||||
28513|Drake Volcanics|70876|5|Briefly described|p2-p3, p64-p75, p79, p81, p96|Permian|Permian|New England Orogen. Additional SHRIMP ages of 265.3 +/- 1.5 Ma (this study) and 264.4 +/- 2.5 Ma (Cross and Blevin, 2010) are provided. This unit was previously included in the Wandsworth Volcanic Group but in this study has been seperated out as a distinct unit on the basis of geochronology. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|265.3 +/- 1.4 Ma (SHRIMP U-Pb)|||||
28513|Drake Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|264+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite, dacite, rhyolite.|
28513|Drake Volcanics|71628|5|Briefly described|p9: 5, 11, 19, 32; p11: 26, 29, 31, 38|||See also p15: 33, 57; p16: 2, 4, 26; p19: 52, 72, 90, 95, 128, 131, 133, 174. RELATED UNITS (continued): Is also intruded by Girard Creek Diorite; Grasstree and Malara Quartz Monzodiorites; Rocky River, Undercliffe Falls Monzogranites (and faulted against the latter); Jenny Lind Tonalite; Cullendore Supersuite; and Mount Carnham Granodiorite (Dumbudgery Creek Complex). Abuts Moonta Gully Monzogranite.|||Navies Creek Member.|Is intruded by Mount Lindesay Monzogranite (Stanthorpe Complex); Morgans Creek Leucomonzogranite; Yellow Gully Leucosyenogranite;  Bruxner and Koreelah Creek Granodiorites; see COMMENTS for more.||
28513|Drake Volcanics|72528|5|Briefly described|p2, p84-85, p110.|Guadalupian|Guadalupian|Situated c. 42 km southeast of Tenterfield.|265.3+/-1.4 to 264.4+/-2.5 Ma|||Intruded by Malara Quartz Monzodiorite.||
28513|Drake Volcanics|73197|5|Briefly described|p475 Fig.6, p477-478, p484|Guadalupian|Guadalupian|New England Orogen, southern. Formed in a shallow shelf environment and is mineralised (Perkins, 1988). U-Pb zircon ages from Carr et al., (2003), Cross and Blevin (2010) and Waltenberg et al., (2016).|265.3 +/- 1.5 Ma, 264.4 +/- 4.0 Ma U-Pb zircon||||Rhyolitic to dacitic volcanics.|
28248|Dregger Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||12-MAY-15
28248|Dregger Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 800. S-Type.||||||
28248|Dregger Granite|24197|5|Briefly described|p77, p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
28248|Dregger Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28248|Dregger Granite|40659|6|Mentioned|p250|||||||||
28248|Dregger Granite|40954|6|Mentioned|p132|||||||||
28248|Dregger Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
28248|Dregger Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
28248|Dregger Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Medium-grained porphyritic garnet-biotite granite.||||||
28248|Dregger Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium-grained porphyritic garnet-biotite granite, contains fayalite in places; fine- to medium-grained biotite granite, commonly porphyritic and garnet-bearing.|
28248|Dregger Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium-grained porphyritic garnet-biotite granite, contains fayalite in places; fine- to medium-grained biotite granite, commonly porphyritic and garnet-bearing.|
28248|Dregger Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Fe-rich granite; contains fayalite and garnet.|
78921|Dresden Limestone Member|65388|4|Described|p160, 162, 164, 165|Artinskian|Artinskian|Of Buffel Formation. A folded sequence of limestone. Up to 50m thick, predominantly limestone, ranging from calcilutite to calcirudite, generally richly fossiliferous. In places it is extensively replaced by chert. Dominant limestone facies is skeletal grainstone and lesser skeletal packstone and rare wackestone.||||||
23560|Drinkwater Diorite|22847|3|Fully described|p 46|Silurian|Ordovician|||||||
23560|Drinkwater Diorite|23422|5|Briefly described|p214 Table 6.8|||||||||
23560|Drinkwater Diorite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
23560|Drinkwater Diorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 126.||||||
23560|Drinkwater Diorite|42245|2|Defined|p34|Early Devonian||||||||
23560|Drinkwater Diorite|43093|4|Described|Appendix 1|Silurian|Ordovician|||||||
23560|Drinkwater Diorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Late Silurian to Early Devonian?.||||||
23560|Drinkwater Diorite|43933|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
23560|Drinkwater Diorite|43935|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
28020|Drovers Lagoon Formation|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Edward River Metamorphic Group||||||12-JAN-05
28020|Drovers Lagoon Formation|22781|4|Described|p17|Proterozoic|Proterozoic|Edward River Metamorphic Group||||||
28020|Drovers Lagoon Formation|23420|5|Briefly described|p 142 table 4.4|||In the Edward River Metamorphic Group. Thickness 800m. Correlates with Sugarbag Creek Formation.||||||
28020|Drovers Lagoon Formation|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|Of Edward River Metamorphic Group.||||||
28020|Drovers Lagoon Formation|43596|4|Described|p16, p20 Tb. 1||Proterozoic|Of the Edward River Metamorphic Group. Conformably overlies Olkolo Formation; conformably overlain by O'Lane Formation. Thickness: ~800m. Lithology ranges from very low grade metamudstone-siltstone-sandstone to quartzite and schist.||||||27-JAN-09
28020|Drovers Lagoon Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Edward River Metamorphic Group||||||24-JAN-05
28020|Drovers Lagoon Formation|69591|5|Briefly described|p78-79 Tb.2.6|||Savannah Province, Coen Inlier. 800m thick. Forms a narrow, elongate band.||Edward River Metamorphic Group.||Correlates with Sugarbag Creek Formation.|Metamudstone, siltstone and sandstone conglomerate; quartzite, slate and phyllite.|
40857|Dry Bore Granite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
40857|Dry Bore Granite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Cream, foliated, medium-grained, equigranular, leucocratic muscovite-biotite granite and pegmatite.|
40857|Dry Bore Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
40868|Dry River Metavolcanics|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Of the Balcooma Metavolcanic Group.  Porphyritic rhyolitic metavolcanics.||||||
40868|Dry River Metavolcanics|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province. A separately-mapped sub-unit has similar lithologies but includes breccia and volcanic arenite and subvolcanic intrusions.||Unit in Balcooma Metavolcanic Group.|||Pink, grey or cream, variably schistose and porphyritic rhyolitic metavolcanics (lava and volcaniclastic rocks); grades into muscovite schist.|
40868|Dry River Metavolcanics|68731|5|Briefly described|p152, p154|Early Ordovician|Early Ordovician|Lithic clasts to pebble size are recognisable. The unit formed from a succession of silicic volcaniclastic rocks, probably along with intrusive rhyolite sills and dykes. Age constrained by the parent Balcooma Metavolcanic Group.||Of the Balcooma Metavolcanic Group.|||Comprises metarhyolite with subordinate metasedimentary rocks. The metarhyolite contains relict phenocrysts of quartz, plagioclase and K-feldspar in a fine-grained groundmass.|
75602|Dryander Granite|69594|5|Briefly described|p567 Fig.7.39|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.||||||
73613|Duckpond Road Metamorphics|68421|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province. U-Pb zircon ages (Carson et al. 2006). The minimum age range represents a metamorphic age, whilst the maximum age represents a detrital age.|318.7 +/- 3.0 Ma, 261 - 286 Ma |||Intruded by the Glen Eva Complex, Conella Granodiorite, Bootoo Creek Granite, Cassillis Granite and Dahls Hills Complex.|Biotite gneiss, migmatitic gneiss and associated granite, mica schist, amphibolite, quartzite; minor pegmatite.|
73613|Duckpond Road Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Broome Head and Gaythorn Metamorphics, Sabina Point Schist, The Shacks Mylonite, Townshend Formation, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
36296|Duffers Creek Dacite|23291|4|Described|p93 Fig. 3.9|Early Permian|Late Carboniferous|Of the Bulleringa Volcanic Subgroup. Age: 289+/-2Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36296|Duffers Creek Dacite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Scardon Volcanic Group.||||||
36296|Duffers Creek Dacite|23616|5|Briefly described|Table 3 p53|||Of Scardons Volcanic Group.||||||
36296|Duffers Creek Dacite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Bulleringa Volcanic Subgroup.|Informally subdivided into two units.||Mainly lithics-poor to lithics-rich, moderately crystal-rich to crystal rich, dacitic ignimbrite; slightly porphyritic dacite, with scattered plagioclase phenocrysts (partly chloritised).|
23563|Duffs Range Granite|23032|4|Described|p14|Early Ordovician|Cambrian|||||||
23563|Duffs Range Granite|23291|4|Described|p89 Fig. 3.8|Ordovician|Ordovician|Intrudes Balcooma Metavolcanics and Lugano Metavolcanics. Intruded by Dido Tonalite (Dido Supersuite - Silurian). Geological Province: Georgetown Region.||||||08-JUL-15
23563|Duffs Range Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 71. I-Type.||||||
23563|Duffs Range Granite|41675|2|Defined|p58|Ordovician||Originally entered as Duff Range Granite [Indexing error corrected by IWWithnall Aug94]||||||
23563|Duffs Range Granite|42693|5|Briefly described|map legend|Proterozoic|Early Paleozoic|Originally reserved & defined as Duffs Range Granite, but indexed as Duff Range Granite in 89/26596.||||||07-NOV-08
23563|Duffs Range Granite|43259|4|Described|Appendix 1,p20.||Ordovician|Ordovician?||||||
23563|Duffs Range Granite|43286|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23563|Duffs Range Granite|50200|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
23563|Duffs Range Granite|68410|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian||||||Pink, strongly foliated, equigranular to porphyritic, fine to coarse-grained biotite granite; pink, locally strongly foliated and mylonitised, equigranular to porphyritic, fine to coarse-grained, biotite granite and granodiorite.|
23563|Duffs Range Granite|68731|6|Mentioned|p151 Fig 3.51|Ordovician|Ordovician|||||||
27686|Dumbano Granite|9541|5|Briefly described|Map legend|Devonian|Silurian|Grey medium-grained biotite granite; abundant megacrysts.||||||
27686|Dumbano Granite|22744|5|Briefly described|P6, P7, Table2 P9|Early Devonian|Late Silurian|||||||
27686|Dumbano Granite|23032|4|Described|p38|Silurian|Silurian|||||||
27686|Dumbano Granite|23220|5|Briefly described|Fig.1|Early Devonian|Late Silurian|of Georgetown Inlier.||||||
27686|Dumbano Granite|23291|5|Briefly described|p35,p89 Tb. 3.8|Silurian|Silurian|Age: 421+/-8Ma. Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27686|Dumbano Granite|23424|5|Briefly described|p346|||Age: 421 +/- 8 Ma.||||||
27686|Dumbano Granite|23429|6|Mentioned|p429|||||||||
27686|Dumbano Granite|23430|5|Briefly described|Table 14.2 p460.||Devonian|K-Ar; Rb-Sr 390-400 Ma. Zircon crystallisation 421+/-8 Ma. Pama Province.||||||
27686|Dumbano Granite|23493|5|Briefly described|p8, p19 Tb. 1|Precambrian|Precambrian|Grey, medium-grained biotite granite wit pink porphyritic feldspar.  Intrudes Einasleigh Metamorphics and Forsayth Granite.||||||
27686|Dumbano Granite|23494|5|Briefly described|p10, p24 Tb, 1|Precambrian|Precambrian|Intrudes Forsayth Granite, Einasleigh Metamorphics; intruded by Butlers Igneous Complex and Lochaber Granite.||||||
27686|Dumbano Granite|23495|5|Briefly described|map legend||Proterozoic|Age shown as Proterozoic?||||||
27686|Dumbano Granite|23498|5|Briefly described|p24 table 1|||Intruded by Bagstowe Igneous Complex. Intrudes Einasleigh Metamorphics and Paddys Creek Formation.||||||
27686|Dumbano Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 37. I-Type.||||||
27686|Dumbano Granite|24013|5|Briefly described|p19 Tb. 1|Proterozoic|Proterozoic|Grey, medium-grained, biotite granite with pink porphyritic feldspars.  Correlated with Robin Hood and Forsayth Granites.  Intrudes Etheridge Formation.  Dyked by Bagstowe Ring Complex||||||
27686|Dumbano Granite|29445|6|Mentioned|p91|||||||||
27686|Dumbano Granite|30257|6|Mentioned|p303|||Also date P303||||||
27686|Dumbano Granite|30587|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
27686|Dumbano Granite|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
27686|Dumbano Granite|31832|6|Mentioned|Table 6|||||||||
27686|Dumbano Granite|31999|6|Mentioned|p138,Tb.II|||||||||
27686|Dumbano Granite|32360|6|Mentioned|p743|||||||||
27686|Dumbano Granite|32528|5|Briefly described|Table 1|||||||||
27686|Dumbano Granite|32531|6|Mentioned|p477|||||||||
27686|Dumbano Granite|32553|4|Described|p60|||||||||
27686|Dumbano Granite|33644|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Sil. - L.Dev.||||||
27686|Dumbano Granite|33648|4|Described|p10|||||||||
27686|Dumbano Granite|35560|6|Mentioned|p288|||||||||
27686|Dumbano Granite|35920|6|Mentioned|p24|||||||||
27686|Dumbano Granite|35930|6|Mentioned|Fig.1|||||||||
27686|Dumbano Granite|36472|6|Mentioned|Map legend|Early Devonian|Late Silurian|Early Devonian to Late Silurian||||||
27686|Dumbano Granite|37570|4|Described|p121|||See also Fig.3||||||
27686|Dumbano Granite|37573|6|Mentioned|p201|||See also Fig.12||||||
27686|Dumbano Granite|37576|5|Briefly described|p8|||||||||
27686|Dumbano Granite|37614|4|Described|p237|||See also P233.||||||
27686|Dumbano Granite|37768|6|Mentioned|p42|||||||||
27686|Dumbano Granite|38715|6|Mentioned|p192|||||||||
27686|Dumbano Granite|39027|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
27686|Dumbano Granite|39445|5|Briefly described|Table 12|||See also P72||||||
27686|Dumbano Granite|39689|6|Mentioned|p51|||||||||
27686|Dumbano Granite|39735|6|Mentioned|p18|||||||||
27686|Dumbano Granite|39917|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
27686|Dumbano Granite|39981|6|Mentioned|p104|||||||||
27686|Dumbano Granite|40787|6|Mentioned|p336|||||||||
27686|Dumbano Granite|41260|6|Mentioned|p48|||||||||
27686|Dumbano Granite|41272|6|Mentioned|M 1of1 A09|||||||||
27686|Dumbano Granite|41675|1|Redefined|p65|Early Devonian||||||||
27686|Dumbano Granite|41680|6|Mentioned|p104|||||||||
27686|Dumbano Granite|42031|5|Briefly described|p764|||||||||
27686|Dumbano Granite|42054|6|Mentioned|p273|||||||||
27686|Dumbano Granite|42279|6|Mentioned|Fig.2 P18|||||||||
27686|Dumbano Granite|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27686|Dumbano Granite|43259|4|Described|Appendix 1,p17.|Early Devonian|Late Silurian|||||||
27686|Dumbano Granite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
27686|Dumbano Granite|43461|14|Not recorded|p616|||||||||
27686|Dumbano Granite|43480|6|Mentioned|4|Devonian|Silurian|||||||
27686|Dumbano Granite|43664|6|Mentioned|p96|||||||||
27686|Dumbano Granite|43978|14|Not recorded|p146-150|||||||||
27686|Dumbano Granite|44043|14|Not recorded|Tb.1,Figs.6,8,p70||Late Precambrian|Intrudes Einasleigh Metamorphics and Bernecker Formation. Unconformably overlain by Bundock Creek Formation.||||||
27686|Dumbano Granite|44047|14|Not recorded|Map Legend||Proterozoic|||||||
27686|Dumbano Granite|44048|14|Not recorded|Map Legend||Proterozoic|||||||
27686|Dumbano Granite|44049|14|Not recorded|Map Legend||Proterozoic|||||||
27686|Dumbano Granite|44059|2|Defined|p442-447|Late Precambrian|Paleoproterozoic|||||||07-NOV-08
27686|Dumbano Granite|44091|14|Not recorded|p31||Early Devonian|||||||
27686|Dumbano Granite|44258|14|Not recorded|p1,7,9,12,16,18,28,||Paleozoic|380 Ma. p29,37,38. (Middle Palaeozoic)||||||07-NOV-08
27686|Dumbano Granite|44259|14|Not recorded|p107|||380+/-8 Ma||||||
27686|Dumbano Granite|44516|14|Not recorded|p34|||||||||
27686|Dumbano Granite|44542|14|Not recorded|p27,28|||||||||
27686|Dumbano Granite|45003|14|Not recorded|p13,36,40,42|||||||||
27686|Dumbano Granite|45009|2|Defined|p101-104,133,Pl.13|||Intrudes Forsayth Granite, Paddys Creek Formation. Intruded by Bagstowe Ring Dyke Complex||||||
27686|Dumbano Granite|45014|14|Not recorded|p73,Pl.19,21||Devonian|||||||
27686|Dumbano Granite|45087|5|Briefly described|p27|||Chem. analyses.||||||
27686|Dumbano Granite|45113|3|Fully described|p7|||Emphasis on petrography. Geochemistry P33.||||||
27686|Dumbano Granite|45151|6|Mentioned|Table 3|||See also Table 5.||||||
27686|Dumbano Granite|48894|6|Mentioned|p38|||See also PP39,49. 379my.||||||
27686|Dumbano Granite|48903|3|Fully described|p22|||U.Sil.-L.Dev. K/Ar age. See also Table 1||||||
27686|Dumbano Granite|48904|6|Mentioned|p17|||||||||
27686|Dumbano Granite|48908|6|Mentioned|p43|||||||||
27686|Dumbano Granite|48914|6|Mentioned|p30|||||||||
27686|Dumbano Granite|48976|6|Mentioned|p5|||||||||
27686|Dumbano Granite|50200|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
27686|Dumbano Granite|50211|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Age: 1550-1560 Ma. Of the Glenmore Batholith.||||||17-MAY-04
27686|Dumbano Granite|60081|5|Briefly described|Map legend|Early Devonian||Grey biotite granite.  Max. age: Late Silurian?||||||
27686|Dumbano Granite|68357|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Glenmore Batholith, Pama Province.|||||Grey, locally foliated, porphyritic biotite granite; grey, locally foliated, muscovite and biotite-muscovite granite.|
27686|Dumbano Granite|68410|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Dumbano Batholith.|||||Grey, locally foliated, muscovite and biotite-muscovite granite and porphyritic biotite granite.|
27686|Dumbano Granite|69592|5|Briefly described|p282|Silurian|Silurian||421 +/- 8 Ma (SHRIMP U-Pb zircon).|White Springs Supersuite.|||I-type.|
27686|Dumbano Granite|71592|5|Briefly described|Appendix A.||||421+/-8 Ma (SHRIMP U-Pb zircon).||||Granite.|
33890|Dumbano Supersuite|22533|6|Mentioned|p54|Early Devonian|Silurian|placed in Pama Province||||||
33890|Dumbano Supersuite|23291|5|Briefly described|p19|Early Devonian|Silurian|Geological Province:  Georgetown Region.||||||08-JUL-15
35548|Dumbleton Rocks Ignimbrite|23162|5|Briefly described|p883|||||||||
39014|Dumgree Suite|23799|5|Briefly described|p115, p117|||Of Murray and others (2000, in prep.).  Includes Dumgree Tonalite, Bundaleer Tonalite and Bajool Quartz Diorite.  Geological Province: Yarrol Province||||||
32047|Dumgree Tonalite|23799|5|Briefly described|p117|||Of Murray and others (2000, in prep.).  Of the Dungree Suite.  Geological Province: Yarrol Province.||||||
32047|Dumgree Tonalite|24491|5|Briefly described|p21|||Previously included as part of Galloway Plains Tonalite.||||||
32047|Dumgree Tonalite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgad].  Pale grey medium-grained leucocratic biotite-hornblende tonalite; grey medium-grained hornblende quartz diorite.||||||
32047|Dumgree Tonalite|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
32047|Dumgree Tonalite|68008|2|Defined|p331, p334-335, p361, p372-373, p375-376|Early Triassic|Permian|See also p378, p380-389, p629. An equidimensional mass c.8km across, 40km NE of Biloela. Named after the property of Dumgree. The type area is along the Gladstone-Moura railway line, from 1.5km S of Mount Redshirt to 2km ENE of Mount Rainbow siding; well-exposed in numerous cuttings. Varied topography (described). Surrounded by Rocky Point Granodiorite. Geophysics described. Geochemistry described and modelled: similar to Bundaleer Tonalite; contrasted with Bocoolima and Rocky Point Granodiorites.|c.244 Ma.|Galloway Plains Igneous Complex.||Intrudes Youlambie Conglomerate and ?Rocky Point Granodiorite. Is intruded by Redshirt Granite.|Ranges from quartz diorite to granodiorite in composition. Tonalite is dominant; lesser trondhjemite; andesite dykes. Local periphery of strongly magnetic diorite and gabbro.|
32047|Dumgree Tonalite|68679|5|Briefly described|p424-425, p427|||Yarrol Province. Western third of the Complex. Forms a single large pluton with the Rocky Point Granodiorite. Geochemistry briefly described.||Galloway Plains Igneous Complex.||Intrudes Youlambie Conglomerate. Is intruded by Redshirt Granite.|Leucocratic biotite-hornblende tonalite to trondhjemite; hornblende-quartz diorite.|
69839|Dunethin Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
69839|Dunethin Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Rhyolite to dacite.|
69839|Dunethin Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
36186|Dunk Island Granite|23497|5|Briefly described|Table 1||Carboniferous|of Kennedy Province. Age: 336+/-5Ma(SHRIMP). Intrudes Barnard Metamorphics.||||||
36186|Dunk Island Granite|23507|5|Briefly described|Map Legend||Early Carboniferous|Age: 336+/-5Ma SHRIMP.||||||
36186|Dunk Island Granite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of Dunk I.Suite. Mafic granite: pale grey, med.-gr., even-gr.to slightly porphyritic biotite granite; with bluish-grey quartz grains scattered lenticular inclusions of biotite gneiss. I-type. IncludesTapp-Ana granite in most recent mapping.||||||07-FEB-11
36186|Dunk Island Granite|68731|6|Mentioned|p160, p161|||||||||
36186|Dunk Island Granite|69593|5|Briefly described|p492, p495, p512|||Kangaroo Hills Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|336 /- 5 Ma.||||Mainly biotite granite and microgranite; minor gabbro. I-type.|
75169|Dunk Island Suite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of Dunk Island Suite (Dunk Island Supersuite) within the Bedarra Granite Belt. Contains Dunk Island Granite. I-type.||||||07-FEB-11
69338|Dunk Island Supersuite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of Dunk Island Suite (Dunk Island Supersuite) within the Bedarra Granite Belt. Contains Dunk Island Suite. I-type.||||||07-FEB-11
69880|Dunollie beds|61761|6|Mentioned|p4|||Geological Province: Philpott Block, Gamilaroi terrane.||||||07-FEB-11
69880|Dunollie beds|64398|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Basalt, andesite, dacite and volcaniclastic siltstone to rudite; minor allochthonous limestone, limestone.||||||14-AUG-08
69880|Dunollie beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Marble Waterhole, Craigilee, Calliope and Munbooree beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
69880|Dunollie beds|68679|5|Briefly described|p312-313, p317, p401|Devonian|Late Silurian|Withnall (1972); Whitaker, Murphy and Rollason (1974). Philpott Subprovince, Northern New England Orogen. Occupies the core of a syncline in the Toondahra Creek area. Age range also given as Early-Middle Devonian.||||Conformably overlies Munbooree beds.|Mainly mafic to intermediate lavas and volcaniclastics; the flows are tholeiitic basalt, plagioclase-phyric andesite and dacite. Minor volcanilithic conglomerate, sandstone and siltstone include rare allochthonous limestone blocks.|
69880|Dunollie beds|73450|6|Mentioned|p36|||||||Intruded by Toondahra Granite.||
77107|Durabilla Formation|63218|6|Mentioned|p211 Fig.2, p212 Fig.3. |Middle Jurassic|Middle Jurassic|Surat Basin.||Unit in Walloon Subgroup.||Overlies Eurombah Formation. Is overlain by Taroom Coal Measures.||
77107|Durabilla Formation|67133|6|Mentioned|p12-14|||Smectite-rich mixed-layer clays.||Walloon Subgroup.||||
77107|Durabilla Formation|68117|4|Described|p346-349, p355|Middle Jurassic|Middle Jurassic|New name: the unit is widespread and lithologically distinct. Eastern Surat Basin. Comprises lithostratigraphic intervals 3 and 4 of Swarbrick (1973) in Injune Creek Group. Has similar lithologies to Taroom Coal Measures, but without significant coal. Distinguished most easily by wireline logs. The top is taken as the base of the Condamine Seam (Taroom Coal Measures).||Walloon Subgroup.||Overlies Eurombah Formation gradationally or, where absent, the Hutton Sandstone. Is overlain gradationally by Taroom Coal Measures.|Interbedded, labile to sublabile sandstones, siltstones and mudstones with rare thin coal bands.|
77107|Durabilla Formation|68139|5|Briefly described|p24-25, 28, 30-33|Middle Jurassic|Middle Jurassic|Surat Basin. In Fig.4, appears as ""Durabilla Formation""/Eurombah Formation. Maceral composition tabulated, discussed.||Walloon Subgroup.||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.|Mainly sandstone; minor coal.|
77107|Durabilla Formation|69574|6|Mentioned|p22, 24|Middle Jurassic|Middle Jurassic|Surat Basin. Presented on p24 as ""Durabilla Formation""/Eurombah Formation.",,||Walloon Subgroup.||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
77107|Durabilla Formation|69594|6|Mentioned|p536|||Scott et al. (2004) separated the basal sandstone unit of the Taroom Coal Measures to constitute this Formation. In this study, it is regarded as a Member of the Walloon Coal Measures only in the NE Surat Basin.||||||
77107|Durabilla Formation|69790|5|Briefly described|p1061, p1066-1078|||Amalgamated, stacked and isolated channel deposits form a laterally continuous transition unit. Includes Eurombah Formation. Thins to the S. Considered to be an important aquitard: of significance in targetting coal seam gas.||Unit in Walloon Subgroup.||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
77107|Durabilla Formation|70374|6|Mentioned|p808, p809, figure 1,|Callovian|Bathonian|Amalgamated with Eurombah Formation in areas where the wireline log responses cannot be distinguished. ||Included in Walloon Subgroup by some, but not shown as part of Walloon Coal Measures.||Included in Walloon Subgroup.||
77107|Durabilla Formation|70628|5|Briefly described|p952,954,958,964,965 Fig 17|Bajocian|Bajocian|||Walloon Subgroup||Underlies Taroom Coal Measures. Overlies Hutton Sandstone.|Coal-barren sedimentary rock.
|29-JUN-16
77107|Durabilla Formation|70725|6|Mentioned|p13|Middle Jurassic|Middle Jurassic|Surat Basin. Is presented as Durabilla/Eurombah Formation.||||Overlies Hutton Sandstone. Is overlain by Taroom Coal Measures.||
77107|Durabilla Formation|71282|5|Briefly described|p456, p457 Fig.1, p459-460, p466 Fig.13|||Heterolithic, fine-grained flood basin sediments.||Basal Injune Creek Group.||Overlies Hutton Sandstone.||
77107|Durabilla Formation|72297|5|Briefly described|p699 Fig.10.11|Jurassic|Jurassic|Surat Basin.||Walloon Subgroup.||||
77107|Durabilla Formation|72921|4|Described|p13, p15 Fig.2, p16-17, p40, p42, p46.|Middle Jurassic|Middle Jurassic|Shown as located in the Surat Basin in Queensland. Acts an aquitard between the Walloon Coal Measures and the Hutton Sandstone.||||Overlies and is equivalent to Hutton Sandstone and is underlying Walloon Coal Measures.||
77107|Durabilla Formation|73113|5|Briefly described|p. 22-24, 29, 31, 36-37, 41, 49...|||Surat Basin. Tight aquitard. More locations: p. 68-69, 79-80, 98, 115-116, 119, 128-129, 148-149, 152, 166, 169-172, 176-177, 179, 191, 193.||||Underlain by Hutton Sandstone. Overlain by Walloon Coal Measures.||
29618|Durong Road Suite|43005|5|Briefly described|p217|||||||||
27394|Durundur Shale|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
27394|Durundur Shale|37252|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27394|Durundur Shale|39445|5|Briefly described|Table 7|||See also P84 & Fig.7||||||
27394|Durundur Shale|40051|6|Mentioned|p5|||||||||
27394|Durundur Shale|43008|5|Briefly described|map legend|||||||||
36289|Dynan Dacite|23291|4|Described|p93 Table 3.9|Early Permian|Early Permian|Parent: Galloway Volcanic Group. Age: 290+3Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36289|Dynan Dacite|23510|5|Briefly described|Map Legend||Early Permian|of Galloway Volcanic Group.||||||
79753|Dynevor Downs formation|70720|5|Briefly described|p8|||No age control. Tabular domain marked by large, elongate areas of reverse magnetisation (origin unknown) parallel to regional trends. May be intersected by GSQ Bulloo 1.|||||Grey/green metasandstone, schist.|24-MAR-17
41262|East Apple Granite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|medium to coarse grained, hornblende-biotite adamellite.||||||
41262|East Apple Granite|65388|2|Defined|p313, p301 Fig 98, p340|Early Triassic|Late Permian|Of Tandora Suite. May extend under Evergreen Formation. Intrudes early Permian Narayen beds. Is overlain by  Jurassic Evergreen Formation. Age uncertain. Pink to brown, fine to medium-grained, porphyritic hornblende-biotite granite in type area.||||||
41262|East Apple Granite|68679|5|Briefly described|p418|||Rawbelle Batholith. Outcrop area ~3 km2; may extend south under cover.||Tandora Suite.||Intrudes Narayen beds.|Hornblende-biotite monzogranite.|
28522|East Boorama Granite|42556|5|Briefly described|Fig.2 P4|||Related to West Boorama Granite?||||||
75642|East Creek Tonalite|67874|6|Mentioned|p50|||Mentioned in analytical session metadata.||||||
75642|East Creek Tonalite|68679|5|Briefly described|p361, p363, p365 Fig.5.51, p366 Fig.5.57|Permian|Permian|Northern Connors Subprovince. Early Permian. Part of the Urannah Batholith. REE plot.|289 +/- 1.7 Ma (U-Pb SHRIMP: Cross et al. 2012).||||I-type. Foliated biotite-hornblende tonalite.|
75642|East Creek Tonalite|68901|5|Briefly described|p3-4, p41, p44-46, p91-93, p144, 146|Cisuralian|Cisuralian|northern New England Orogen, Bowen Region. 2 samples dated, a foliated quartz diorite and a granodiorite. SHRIMP age is interpreted as the age of magmatic crystallisation. An additional SHRIMP age of 289.4 +/- 1.7 Ma and lithological description is provided. SHRIMP results and analysis discussed in detail.|292.5 +/- 1.9 Ma (SHRIMP U-Pb)|||Contact with Key Creek Gneiss sought but not found. Age compared with leucotonalite lens in Key Creek Gniess.|Pale-grey, medium-grained, slightly uneven grained, foliated hornblende-biotite quartz diorite with traces of K-feldspar and titanite. Pale grey, medium-grained, slightly porphyritic biotite granodiorite.|28-SEP-18
75642|East Creek Tonalite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|293+/-1.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite.|
75642|East Creek Tonalite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, medium-grained, uneven-grained to slightly porphyritic hornblende-biotite + biotite tonalite; hornblende-biotite, biotite-hornblende, + biotite granodiorite; + subordinate grey fine to medium-grained (biotite-) hornblende quartz diorite.|
23569|Eastdale Granite|23032|4|Described|p44,45||Carboniferous|||||||
23569|Eastdale Granite|23291|4|Described|p50, p98 Tb. 3.11|Carboniferous|Carboniferous|Intruded by the Lochaber Granite. Geological Province: Georgetown Region.||||||08-JUL-15
23569|Eastdale Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 36. Assumed to be I-Type.||||||
23569|Eastdale Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23569|Eastdale Granite|40542|6|Mentioned|p97|||||||||
23569|Eastdale Granite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
23569|Eastdale Granite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
23569|Eastdale Granite|43664|6|Mentioned|p83||Carboniferous|||||||
23569|Eastdale Granite|43740|4|Described|p27||Carboniferous|||||||
23569|Eastdale Granite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23569|Eastdale Granite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Pink, medium to coarse-grained biotite granite.|
23569|Eastdale Granite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Biotite granite. I-type.|
30694|Easter Egg Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30694|Easter Egg Granite|50536|5|Briefly described|p1.4, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30694|Easter Egg Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite|||Foliated coarse porphyritic biotite granite; porphyritic quartz diorite with quartz ocelli|
30694|Easter Egg Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Foliated porphyritic biotite granite; porphyritic quartz diorite with quartz ocelli.|
35370|Eastern Selwyn Range Early Granite Suite|23192|6|Mentioned|Fig.2|||||||||
35370|Eastern Selwyn Range Early Granite Suite|23967|6|Mentioned|p1331 Fig.1|||||||||
35370|Eastern Selwyn Range Early Granite Suite|24255|5|Briefly described|p32 Fig.1|||Geological Province: Eastern Succession, Mount Isa Block.||||||
35370|Eastern Selwyn Range Early Granite Suite|24256|5|Briefly described|p50 Fig.2|||Age: ca.1545Ma. Geological Province: Mount Isa Block.||||||
35370|Eastern Selwyn Range Early Granite Suite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
35370|Eastern Selwyn Range Early Granite Suite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
35370|Eastern Selwyn Range Early Granite Suite|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
35370|Eastern Selwyn Range Early Granite Suite|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks.||||||
35370|Eastern Selwyn Range Early Granite Suite|65396|5|Briefly described|p53, p78|Calymmian|Calymmian|Eastern Mount Isa Block.|c.1545 Ma.|||||
33939|Eastwood Formation|22518|6|Mentioned|p 10|||In the Adavale Basin.||||||21-OCT-08
33939|Eastwood Formation|23522|5|Briefly described|p250 Fig 6|Eifelian|Emsian|||||||
33939|Eastwood Formation|62985|5|Briefly described|p16|Emsian|Emsian|Contains quartzose and sub-labile sandstones interbedded with siltstone and mudstone; fluvial. Unconformably overlies Gumbardo Volcanics. Geol. prov: Adavale Basin.||||||07-FEB-08
33939|Eastwood Formation|65214|6|Mentioned|p275, p278|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
30177|Eastwood beds|43105|5|Briefly described|Fig.5,p10|||||||||
30177|Eastwood beds|43213|6|Mentioned|p93|Eifelian|Emsian|Adavale Basin. Fluviatile to lacustrine and deltaic.||||Overlies Gumbardo Formation.||
30177|Eastwood beds|64783|3|Fully described|p91-92, 82, 84, 89, 90, 93,94, 104|Emsian|Emsian|Late Emsian. First decribed by Logan (1977) in core from PPC Carlow-1; named by Paten (1977). Informal reference section is 2053 to 3280 m. Includes palynofloras with no recognized counterparts in Australia.||||Unconformably overlies Gumbardo Formation. Is unconformably overlain by Lissoy Sandstone and Cooladdi Dolomite.|Fluvial unit containing quartzose and sub-labile feldspathic sandstone, interbedded and interlaminated with siltstone and mudstone.|15-NOV-17
30177|Eastwood beds|67402|5|Briefly described|p167, p168 tbl ADV/WRR1|Emsian|Emsian|Adavale Basin. Deposited in fluvio-lacustrine depositional environments. See also p170, fig ADV/WRR8, p173 tbl ADV/WRR2, p175.  ||||Overlies the Gumbardo Formation. Overlain by the Log Creek Formation.|Quartz to sub-labile feldspathic sandstones, interbedded and interlaminated with siltstone and mudstone.|
30177|Eastwood beds|68731|5|Briefly described|p177 Fig 3.91, pp180-181 Tb 3.3|Early Devonian|Early Devonian|Adavale Basin. Interpreted fluvial to lacustrine depositional environment (Paten 1977). In contrast, Logan (1977) interpreted deltaic and pro-deltaic-slope environments. From 32.4 m to 227 m thick.|||||Comprises quartz to sublabile feldspathic sandstones interbedded and inter-laminated with dark siltstone and mudstone. Sandstones typifying the unit are generally light grey-green.|10-MAY-16
30177|Eastwood beds|69541|5|Briefly described|p645 Fig.1(b), p654|Emsian|Emsian|Thomson Orogen. Adavale Basin.||||Overlies Gumbardo Formation.|Sandstone, siltstone and mudstone.|
37169|Eatonvale Formation|23522|5|Briefly described|p250 Fig 6|Frasnian|Eifelian|||||||
37169|Eatonvale Formation|65214|6|Mentioned|p278, p282|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23570|Ebagoola Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23570|Ebagoola Granite|22781|4|Described|p34|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
23570|Ebagoola Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Age: 390 Ma, 400 Ma||||||
23570|Ebagoola Granite|42610|2|Defined|p16|Early Devonian|Early Devonian|Approx. 400Ma. Assumed similar age to Kintore Granite.||||||
23570|Ebagoola Granite|43738|6|Mentioned|p5|||||||||
23570|Ebagoola Granite|69592|5|Briefly described|p282|||Cape York Peninsula Batholith.|395 +/- 4 Ma (SHRIMP U-Pb zircon).|Kintore Supersuite.||||
23570|Ebagoola Granite|71031|6|Mentioned|p15, p20, p26, p32-p33||||ca 400 Ma (390 +/- 5 Ma)|||Intrudes the Flyspeck Granodiorite.||
23570|Ebagoola Granite|71592|5|Briefly described|Appendix A.|||Palma Igneous Province.|395+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
23570|Ebagoola Granite|71849|6|Mentioned|p8, p155-156, p195|Devonian|Devonian|||Ebagoola Suite.||||
23570|Ebagoola Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||White to pale cream or pink garnet +/- biotite-muscovite leucogranite, pegmatite, and aplite.|
27766|Ebagoola Suite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Kintore Supersuite||||||12-JAN-05
27766|Ebagoola Suite|22781|4|Described|p30|Paleozoic|Paleozoic|Kintore Supersuite||||||07-NOV-08
27766|Ebagoola Suite|23420|4|Described|p 149 table 4.8||Early Devonian|Also see p 147 table 4.6. In the Kintore Supersuite.||||||
27766|Ebagoola Suite|23430|6|Mentioned|p485|||||||||
27766|Ebagoola Suite|42610|4|Described|p6|||NOT variation on Ebagoola Granite. Part of Kintore Supersuite. Igneous equivalent to Group?||||||
27766|Ebagoola Suite|42640|6|Mentioned|p9|||of Kintore Supersuite||||||
27766|Ebagoola Suite|42650|6|Mentioned|p15|||||||||
27766|Ebagoola Suite|43596|4|Described|p34, p26 Tb. 2, p27 Tb. 3|||Of Kintore Supersuite. Contains 13 named granites.  These are two-mica granites that are commonly leucocratic and associated with abundant pegmatite and mior aplite. More lithological detail presented.||||||15-JAN-09
27766|Ebagoola Suite|43738|5|Briefly described|p5|Devonian|Silurian|||||||
27766|Ebagoola Suite|43741|6|Mentioned|p7,21|Devonian|Silurian|||||||
27766|Ebagoola Suite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Kintore Supersuite||||||24-JAN-05
27766|Ebagoola Suite|71849|5|Briefly described|p2-3, p8, p13-14, p61, p63, p81, p84|Devonian|Devonian|See also p86, p94, p102, p104, p111, p148-159, p161-162, p184, p195. Coen Inlier. Geochemistry detailed.||Kintore Supersuite.|Burns, Ebagoola, Geikie, Heneage, Keane, Kintore, McIlwraith, Tadpole, Vardon Granites.||Mainly medium-grained muscovite-biotite granodiorite or tonalite to muscovite-biotite and biotite-muscovite granite and leucogranite;  even-grained to highly porphyritic. S-type.|
27766|Ebagoola Suite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|McIlwraith Granite.|||
27766|Ebagoola Suite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|Barwon, Burns, Ebagoola, Geikie, Heneage, Keane, Kintore, McIlwraith, Tadpole, Vardon Granites.|||
25890|Eborac Ignimbrite|23421|4|Described|p159.||Late Carboniferous|of Torres Strait Volcanic Group. Thickness: +100m. Intruded by Badu Suite.||||||
25890|Eborac Ignimbrite|32564|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
25890|Eborac Ignimbrite|33880|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25890|Eborac Ignimbrite|33883|6|Mentioned|p9|||||||||
25890|Eborac Ignimbrite|34582|2|Defined|Table 1|Permian|Carboniferous|Carboniferous - Permian||||||
25890|Eborac Ignimbrite|43567|5|Briefly described|p402|||||||||
25890|Eborac Ignimbrite|45076|4|Described|p37|||Carb.?||||||
25890|Eborac Ignimbrite|71031|5|Briefly described|p2-p3, p38, p41, p43|Early Carboniferous|Early Carboniferous|Oriomo Province. ||Torres Strait Volcanic Group||(potentially) Intruded by the Torres Strait Volcanic Group. Overlain by the Endeavour Strait Ignimbrite.||
25890|Eborac Ignimbrite|72983|6|Mentioned|p5, p61-62, p64|||A 353.4 +/- 2 Ma feldspar-quartz porphyry dyke is reported at the approx. contact with the overlying Endeavour Strait Ignimbrite.||Torres Strait Volcanic Group||Overlain by the Endeavour Strait Ignimbrite.||
36304|Eden Vale Rhyolite|23291|4|Described|p92 Fig. 3.9|Late Carboniferous|Late Carboniferous|See also Eden Vale Volcanics. Of the Silent Creek Volcanic Group. Thickness: at least 50m. Geological Province: Georgetown Region.||||||08-JUL-15
36304|Eden Vale Rhyolite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
27395|Edgecumbe beds|24467|5|Briefly described|p379, 394|||See also Edgecumbe Beds. Geological Province: New England Fold Belt.||||||21-OCT-08
27395|Edgecumbe beds|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27395|Edgecumbe beds|42281|5|Briefly described|p71|||||||||
27395|Edgecumbe beds|45151|6|Mentioned|p11|||||||||
27395|Edgecumbe beds|60705|6|Mentioned|p646|||See also Edgecumbe Beds. Geological Province: northern New England Fold Belt.||||||11-APR-05
27395|Edgecumbe beds|64315|5|Briefly described|p525|Early Carboniferous|Early Carboniferous|Geological province: Drummond Basin. Open marine sediments.||||||21-OCT-08
27395|Edgecumbe beds|65388|5|Briefly described|p69|Visean|Tournasian|May be a continuation of Campwyn Volcanics succession in Proserpine sheet area.||||||
27395|Edgecumbe beds|65706|4|Described|Tb.1 p14,15,17,18,19; p62|Early Carboniferous|Early Carboniferous|Equivalent to upper part of Campwyn Volcanics. Limestone deposit at Ben Lomond Hill.||||Unconformably underlies Proserpine Volcanics and probably Airlie Volcanics; upfaulted against Carmila beds.|Shale, greywacke, limestone, acid to intermediate flows, pyroclastics and volcaniclastics, feldspathic and clayey sandstone, siltstone, pebble conglomerate, with minor lithic sandstone and limestone.|
27395|Edgecumbe beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Campwyn Subprovince. This unit is mapped with the Campwyn Volcanics under the symbol, DCw.||||||
27395|Edgecumbe beds|68679|5|Briefly described|p347-348, p360, p363-364|Tournaisian|Tournaisian|Clarke et al. (1971). Crops out between Proserpine and Edgecumbe Bay. Strikes NNW and dips to the E. Thickness up to 6,000m, but may involve fault or thrust repetition. The shale and siltstone are richly and diversely fossiliferous (Tournaisian). The isotopic and fossil ages both militate against a proposed correlation with the upper Campwyn Volcanics.|348.6 +/- 2.8 Ma (SHRIMP U-Pb: Cross et al., 2012)|||Is faulted against Carmila beds (to the W) and probably the Airlie Volcanics to the E.|Shale, volcanilithic and feldspathic sandstone, siltstone, pebble conglomerate, and thin-bedded and fossiliferous to thick-bedded and oolitic limestone; andesitic to rhyolitic lava and volcaniclastic rocks are also presnt.|
27395|Edgecumbe beds|68901|5|Briefly described|p12-16, p1-4, p144||Carboniferous|northern New England Orogen, Bowen Region. SHRIMP age is the date of magmatic crystallisation of a rhyolitic ignimbrite sample. Stratigraphic location of sample within Edecumbe beds is unclear. SHRIMP results and analysis discussed in detail. Parts of this unit previously mapped as Carmila beds.|348.6 +/- 2.8 Ma (SHRIMP U-Pb)|||Intruded by Flagstaff Hill Granite.|Rhyolitic ignimbrite.|27-SEP-18
27395|Edgecumbe beds|69582|5|Briefly described|p41, p45|Early Carboniferous|Early Carboniferous|Campwyn Subprovince. Beds are vertical to very steeply dipping towards the east-northeast. Outcrops along the northeastern side of the Hillsborough basin.||||Broadly equivalent to the Campwyn Volcanics.|Felsic to intermediate lava and tuff with shale, sandstone and limestone deposited in shallow marine and fresh-water environments.|
27395|Edgecumbe beds|69594|6|Mentioned|p558|Carboniferous|Carboniferous|||||Is intruded by Ben Lomond Granite.||
27395|Edgecumbe beds|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|New England Orogen.||||||
27395|Edgecumbe beds|70673|6|Mentioned|p9|Early Carboniferous|Late Devonian|||||||
27145|Edie Tuff Member|30915|6|Mentioned|p100|||||||||
27145|Edie Tuff Member|31122|2|Defined|p350|Early Permian|Early Permian|||||||
27145|Edie Tuff Member|31258|6|Mentioned|Table 1|||||||||
27145|Edie Tuff Member|31860|6|Mentioned|p280|||||||||
27145|Edie Tuff Member|33372|5|Briefly described|p16|||See also P22. From wells.||||||
27145|Edie Tuff Member|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
27145|Edie Tuff Member|36921|6|Mentioned|p175|||See also Table 1.||||||
27145|Edie Tuff Member|37610|6|Mentioned|Fig.3|||||||||
27145|Edie Tuff Member|39478|6|Mentioned|Table 1|||||||||
27145|Edie Tuff Member|41116|5|Briefly described|p431|||See also Table 1||||||
27145|Edie Tuff Member|41198|6|Mentioned|Table 1|||||||||
27145|Edie Tuff Member|42446|4|Described|p7|||||||||
27145|Edie Tuff Member|42474|6|Mentioned|p25|||||||||
27145|Edie Tuff Member|42547|5|Briefly described|p80|||||||||
27145|Edie Tuff Member|43105|5|Briefly described|p13|||of Jochmus Formation||||||
27145|Edie Tuff Member|43114|5|Briefly described|p6|||of Jochmus Formation||||||
27145|Edie Tuff Member|43812|6|Mentioned|Fig.3,p145|||||||||
27145|Edie Tuff Member|46849|6|Mentioned|Fig. 7|||||||||
27145|Edie Tuff Member|66188|6|Mentioned|443, Fig 3,17|Early Permian|Late Carboniferous|Galilee Basin||||||
27145|Edie Tuff Member|68731|6|Mentioned|p198, p201 Fig 3.110|Cisuralian||Comprises a mudstone-siltstone-tuff unit with less significant sandstone in the middle of the formation (Gray and Swarbrick 1975; Swarbrick and Wallin 1976). Varves and tuff occur in outcrop in the southern part of the basin (van Heeswijk 2006).||Unit in Jochmus Formation.|||Mudstone-siltstone-tuff unit with less significant sandstone.|03-JUL-14
27145|Edie Tuff Member|71265|5|Briefly described|p589|Asselian|Asselian|Galilee Basin.||Jochmus Formation.||||
27145|Edie Tuff Member|71701|5|Briefly described|p155-p158, p167-p170|Sakmarian|Asselian|Central Western Area, Eastern Area, Galilee Basin. Dated by CA-IDTIMS at 296.09 +/- 0.07 Ma and 295.65 +/- 0.07 Ma.  Intersected in GSQ Muttaburra 1, CRD Montani 1, OEC Glue Pot Creek 1 and GSQ 1-1A.||Jochmus Formation||Overlain by the Colinlea Sandstone.||
27145|Edie Tuff Member|71710|5|Briefly described|p370, p378,  p379, p381, p385 Fig 21|Early Permian|Early Permian|Geological province: northern Galilee Basin. Widely distributed, distinct well log signatures.||Of Jochmus Formation. With lower Jochmus Formation, forms sequence 4.||Overlies the lower Jochmus Formation. Gradationally overlain by the upper Jochmus Formation.|Floodplain sediments with restricted, high sinuosity fluvial-channel fill that fines upwards to fine-grained carbonaceous mudstone, carbonaceous siltstone and sandstone.|22-MAY-19
27145|Edie Tuff Member|72088|5|Briefly described|p8, p17|Sakmarian|Sakmarian|Eastern Galilee Basin.||Jochmus Formation|||Tuffaceous rocks.|
27145|Edie Tuff Member|73163|5|Briefly described|p467, p472|Asselian|Asselian|Galilee Basin. Found in the upper part of the Jochmus Formation. May be related to the Camboon Volcanics or the Lizzie Creek Volcanics. Ages include 294.91 +/- 0.09 Ma, 294.80 +/- 0.08 Ma, from Muttaburra 1; 295.65 +/- 0.07 Ma, 296.09 +/- 0.07 Ma from Koburra Trough area, with age differences suggesting erosion of the top of the unit on the eastern side of the basin.|294.80 +/- 0.08 Ma - 296.09 +/- 0.07 Ma.|Top of Jochmus Formation.|||Siltstone, mudstone, and tuff.|
27145|Edie Tuff Member|73472|6|Mentioned|p115|Sakmarian|Sakmarian|Galilee Basin.||Jochmus Formation, Joe Joe Group||||
27145|Edie Tuff Member|73495|6|Mentioned|p500|Sakmarian|Sakmarian|||Jochmus Formation|||Includes mudstone, siltstone, and tuff.|
70430|Edinburgh Mountains Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70430|Edinburgh Mountains Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pale grey, medium to coarse-grained, moderately porphyritic hornblende-biotite monzogranite.|
70430|Edinburgh Mountains Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pale grey, medium- to coarse-grained, porphyritic hornblende(?) biotite monzogranite.|
23571|Edmonds Creek Rhyolite|23032|5|Briefly described|p43||Carboniferous|||||||
23571|Edmonds Creek Rhyolite|23291|4|Described|p91 Fig. 3.9|Carboniferous|Carboniferous|Parent: Butlers Volcanic Group. Age: About 330Ma. Thickness: Up to 60m. Geological Province: Georgetown Region.||||||08-JUL-15
23571|Edmonds Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V34. I-Type.||||||
23571|Edmonds Creek Rhyolite|23619|4|Described|p32 Table 1||Carboniferous|Butlers Volcanic Group. Overlying unit McLennons Creek Rhyolite. Underlying unit Einasleigh Metamorphic - unconformable + Ballynure Rhyolite.||||||
23571|Edmonds Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23571|Edmonds Creek Rhyolite|40542|6|Mentioned|p97|||||||||
23571|Edmonds Creek Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Butlers Volcanic Group.||||||
23571|Edmonds Creek Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Butlers Volcanic Group||||||
23571|Edmonds Creek Rhyolite|43259|4|Described|Appendix 1,p4.||Carboniferous|of Butlers Volcanic Group.||||||
23571|Edmonds Creek Rhyolite|43286|5|Briefly described|Map Legend||Carboniferous|of Butlers Volcanic Group.||||||
23571|Edmonds Creek Rhyolite|43740|4|Described|p24|||||||||
23571|Edmonds Creek Rhyolite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Butlers Volcanic Group.||||||
23571|Edmonds Creek Rhyolite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Butlers Volcanic Group.||||||
23571|Edmonds Creek Rhyolite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|||Unit in Butlers Volcanic Group.||Is conformably overlain by McLennons Creek Rhyolite.|Brown to purple, sparsely porphyritic rhyolitic lava.|
23571|Edmonds Creek Rhyolite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure.||Of the Butlers Volcanic Group.||Conformably overlain by the McLennons Creek Rhyolite. Conformably underlain by the Ballynure Rhyolite.|Brown to purple, sparsely porphyritic rhyolitic lava.|
26533|Eidsvold Complex|23037|6|Mentioned|p43,4||Late Permian|Spelling - see Igneous Complex p27.||||||21-OCT-08
26533|Eidsvold Complex|33774|3|Fully described|p63|||Strat. p28.||||||21-OCT-08
26533|Eidsvold Complex|36333|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic.||||||19-AUG-08
26533|Eidsvold Complex|36926|6|Mentioned|p160|||||||||
26533|Eidsvold Complex|39445|5|Briefly described|Table 12|||See also p113.||||||21-OCT-08
26533|Eidsvold Complex|39632|6|Mentioned|p213|||||||||
26533|Eidsvold Complex|41272|5|Briefly described|M 1of1 A15|||||||||
26533|Eidsvold Complex|43008|5|Briefly described|map legend|||||||||
26533|Eidsvold Complex|61087|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Ceratodus Granite, Harkness Granodiorite, Mount Rose Gabbro.||||||
26533|Eidsvold Complex|61832|5|Briefly described|p186|Triassic|Triassic|Part of the Rawbelle Batholith.  Hosts gold deposits.||||||03-JUL-06
26533|Eidsvold Complex|64399|5|Briefly described|Map legend|Late Permian|Late Permian|Includes Mount Rose Gabbro, Harkness Granodiorite, Ceratodus Granite and an unnamed leucocratic biotite granite.||||||21-OCT-08
26533|Eidsvold Complex|65388|3|Fully described|p288-289, 41, 42, 265, 292, 236, 294|Early Permian|Early Permian|Intrudes Nogo beds. Includes Mount Rose Gabbro, Harkness Granodiorite, Ceratodus Granite. Unconformably overlain by the Evergreen Formation, here the basal unit of the Mulgildie Basin. Hosts gold mineralisation. Age of mineralisation (K-Ar on sericite) 269+/-5 Ma, provides min age for unit.  See also p295, 298-299, 300.||||||
26533|Eidsvold Complex|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince.||||||
26533|Eidsvold Complex|68679|4|Described|p312, p344, p353, p404, p406, p408, p415|Permian|Permian|Auburn Subprovince, northern New England Orogen. Has strongly hornfelsed the Nogo beds. Hosts hydrothermal alteration and gold mineralisation. Age determination by Leadbeatter (1992). Other ages given.|269 +/- 5 Ma minimum (K-Ar sericite).||Mount Rose Gabbro, Harkness Granodiorite, Ceratodus Granite.|Intrudes the Nogo beds.|Major rock types are leucogranite, granite, granodiorite, gabbro and diorite; the last two occur in net-vein association with granite.|
24945|Eight Mile Creek beds|39252|6|Mentioned|p22|||||||||
24945|Eight Mile Creek beds|43008|5|Briefly described|map legend|||||||||
24945|Eight Mile Creek beds|61392|5|Briefly described|p164 Fig. 1|Late Permian|Middle Permian|Of the Wildash Group.||||||07-FEB-11
24945|Eight Mile Creek beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Intermediate to acid lava, tuff and agglomerate. Conglomerate, well sorted to pebbly lithic arenite, siltstone and mudstone; richly fossilierous. Basaltic and andesitic to dacitic lava.||||||13-DEC-07
24945|Eight Mile Creek beds|63748|4|Described|p7 Fig. 3, p8, p19|Early Permian|Early Permian|Olgers et al (1974); now incl. some former Connolly Volcanics rocks (Van Noord 1999b). Conformable on Bromley Hills Fm along its northern border; unconformable on Silverwood Gp and Wallaby beds; unconformable below Marburg Subgroup. Detailed lithology.||||||07-FEB-11
24945|Eight Mile Creek beds|68679|5|Briefly described|p446-447, p452|Permian|Permian|Olgers et al. (1974); Dennis (1974). Extended by Van Noord (1999) to include parts of the Connolly Volcanics. Silver Spur Subprovince, Woolomin Province. Occurs 15km S of Warwick in a small, ~8 km2 outlier.||Wildash Group.||Overlies Bromley Hills Formation and (unconformably) the Wallaby beds. Unconformably overlies or is faulted against Silverwood Group. Is overlain unconformably by the Marburg Subgroup.|Mainly sedimentary lower half: conglomerate, pebbly lithic sandstone, well-sorted lithic sandstone, siltstone and mudstone; a rich early Permian marine fauna. The upper half comprises felsic to intermediate volcaniclastic rocks and lavas.|
80895|Eight Mile Granite|69593|5|Briefly described|p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.||||I-type.|
23575|Eland Metavolcanics|23032|4|Described|p14||Early Paleozoic|||||||07-NOV-08
23575|Eland Metavolcanics|23291|4|Described|p35|Ordovician|Cambrian|Geological Province: Georgetown Region.||||||08-JUL-15
23575|Eland Metavolcanics|23430|5|Briefly described|p469|||Referred to as in Lucky Metamorphic Group + Lucky Creek Metamorphic Group (one in the same). Of Lucky Metamorphic Group. Thalanga Province.||||||
23575|Eland Metavolcanics|23431|5|Briefly described|p532|||Of Lucky Creek Metamorphic Group. Thalanga Province.||||||
23575|Eland Metavolcanics|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Volcanic No. V40.||||||
23575|Eland Metavolcanics|23619|4|Described|p35 Table 1||Early Paleozoic|Strongly deformed. Also see p6. Of Lucky Creek Metamorphic Group. Overlying unit Paddys Creek Phyllite. Georgetown Province.||||||07-NOV-08
23575|Eland Metavolcanics|24577|6|Mentioned|p755 Fig. 2|Early Paleozoic|Proterozoic|||||||07-NOV-08
23575|Eland Metavolcanics|41675|2|Defined|p47|Early Paleozoic||||||||07-NOV-08
23575|Eland Metavolcanics|42054|6|Mentioned|p272|||||||||
23575|Eland Metavolcanics|42279|4|Described|p17|||See also Fig.2||||||
23575|Eland Metavolcanics|42407|5|Briefly described|p34|||See also Fig.22 P30||||||
23575|Eland Metavolcanics|42692|5|Briefly described|map legend|Ordovician|Cambrian|||||||
23575|Eland Metavolcanics|42693|5|Briefly described|map legend|Proterozoic|Early Paleozoic|||||||07-NOV-08
23575|Eland Metavolcanics|43113|4|Described|Table 1 p22|||probably early Palaeozoic (Ordovician?).Of Lucky Creek Metamorphic Group.||||||
23575|Eland Metavolcanics|43253|5|Briefly described|map legend|Ordovician|Cambrian|of Lucky Creek Metamorphic Group||||||
23575|Eland Metavolcanics|43259|4|Described|Appendix 1,p4.||Ordovician|of Lucky Creek Metamorphic Group. Age around Ordovician?||||||
23575|Eland Metavolcanics|43286|5|Briefly described|Map Legend|Ordovician|Cambrian|of Lucky Creek Metamorphic Group.||||||
23575|Eland Metavolcanics|43664|6|Mentioned|Fig.3,p15|||||||||
23575|Eland Metavolcanics|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|||||||
23575|Eland Metavolcanics|67455|4|Described|pp575-577, p584 Fig.7.|Ordovician|Cambrian|Lucky Creek domain, Greenvale Province. Has intense foliation dipping steeply to NW. Metamorphic grade decreases eastwards. Chlorite, actinolite and muscovite in greenschist facies. Local dextral shear bands imply west-over-east transport. Calc-alkaline signature. An overall extensional backarc setting, to the west of a subduction-related arc, is inferred.||Unit in Lucky Creek Metamorphic Group.|||Mafic to silicic volcanic and volcaniclastic rocks derived from feldspathic sandstone, breccia, conglomerate, chert and limestone.|
23575|Eland Metavolcanics|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Lucky Creek Metamorphic Group.|||Chlorite and actinolite schist (meta-andesite to dacite) with common relict plagioclase phenocrysts or clasts, volcaniclastic meta-arenite and meta-rudite, muscovite schist, phyllite and minor marble; locally mylonitic.|
23575|Eland Metavolcanics|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Lucky Creek Metamorphic Group.|||Chlorite and actinolite schist (meta-andesite to dacite) with common relict plagioclase phenocrysts or clasts, volcaniclastic meta-arenite and meta-rudite, muscovite schist, phyllite and minor marble; locally mylonitic.|
23575|Eland Metavolcanics|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.|||||Chlorite and actinolite schist (meta-andesite to dacite) with common relict plagioclase phenocrysts or clasts, volcaniclastic meta-arenite and meta-rudite, muscovite schist, phyllite and minor marble; locally mylonitic; metachert (separately mapped)|
23575|Eland Metavolcanics|68576|5|Briefly described|Q_11: p33-35|||Age and relationships uncertain; probably Cambrian or Ordovician; may be correlative of Seventy Mile Range Group.||Lucky Creek Metamorphic Group.|||Mostly volcaniclastic rocks of andesitic to dacitic composition with calc-alkaline affinities; strongly deformed and metamorphosed to chloritic and actinolite schists. Have shallow-dipping foliation and a stretching lineation.|
23575|Eland Metavolcanics|68731|5|Briefly described|p151 Fig 3.51, p153 Fig 3.52, p155, p158|Ordovician|Ordovician|Ranges from mafic to dacitic with a calc-alkaline affinity. Lacking isotopic ages as no zircon has been found in the Eland Metavolcanics. Mainly upper greenschist grade.||Of the Lucky Creek Metamorphic Group.||Overlain by the Lugano Metamorphics. Overlain and underlain by the Paddys Creek Phyllite.|Comprises mainly fine-grained, green, chlorite-albite schist that also contains actinolite, minor quartz, muscovite, epidote, calcite, titanate and opaque oxides.|
23575|Eland Metavolcanics|69079|5|Briefly described|p60|||Hosts gold mineralisation in quartz veins in the the Lucky Creek Goldfield.||Lucky Creek Metamorphic Group||Is intruded by Dido Tonalite.||
79124|Eldorado Clastics Member|70913|4|Described|p8 fig 3, p10, p35-p37, p67 fig 9, App 1|Middle Permian|Early Permian|Gympie Province. Named for the Eldorado Road. Discussed as a Member of the Rammutt Formation but often abbreviated to Eldorado Clastics (p24, 31, 34, 35,36,41, 87). Replaces the informal Lower Nash clastics. Equivalent to Second Slate Group of Dunstan (1911). Reference sections are briefly mentioned. Distribution briefly described. Up to 20m thick.||Rammutt Formation||Conformably overlies the Mary Basalt and the Tozer Basalt Member. Overlain by the Calton Andesite Member.|Medium-grained, volcanoclastic, hematitic sandstone and pebble conglomerate.|15-SEP-17
24263|Eleven-B Granite|23291|4|Described|p89 Fig. 3.8|Llandovery|Llandovery|Parent: White Springs Supersuite. Age: 426+/-4Ma. Geological Province: Georgetown Region.||||||11-MAY-15
24263|Eleven-B Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 59. I-Type.||||||
24263|Eleven-B Granite|23619|4|Described|p41 Table 2|Early Devonian|Silurian|Intrudes Einasleigh Metamorphics. Copperfield Batholith Province.||||||
24263|Eleven-B Granite|39981|2|Defined|p102|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||11-MAY-15
24263|Eleven-B Granite|40542|6|Mentioned|p98|||||||||
24263|Eleven-B Granite|41680|3|Fully described|p120|||||||||
24263|Eleven-B Granite|43113|4|Described|Table 2 p26|||Probably Silurian to Early Devonian.||||||
24263|Eleven-B Granite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24263|Eleven-B Granite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
24263|Eleven-B Granite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
24263|Eleven-B Granite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Unit in Copperfield Batholith. |||||Foliated, pink to grey, equigranular to porphyritic biotite-muscovite granite.|
24263|Eleven-B Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
74937|Elgin Vale Diorite|65668|5|Briefly described|p2 Tb.1, p19-22|Triassic|Triassic|New name for a series of dominantly dioritic intrusions into Neara Volcanics. Previously mapped as un-named unit Rgd in Nanango 1:100 000 sheet, in which it was described as equigranular to porphyritic microdiorite, porphyritic microdiorite, biotite-hornblende diorite. Gympie area; New England Orogen. Age: 235.2 +/- 2.4 Ma (SHRIMP U-Pb zircon). Problems with previous dating results discussed.||||||
74937|Elgin Vale Diorite|68679|5|Briefly described|p391, p409, p411|||A newly-recognised unit in this area adjacent to the E margin of the Esk Basin.|235.2 +/- 2.4 Ma (SHRIMP U-Pb: Cross et al. 2009).|||Intrudes Neara Volcanics.|Hornblende microdiorite, diorite to granodiorite and gabbro.|
74937|Elgin Vale Diorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|235+/-2.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
35080|Elimeek Volcanics|23049|3|Fully described|p70|||||||||
35080|Elimeek Volcanics|23283|2|Defined|p30|Permian|Carboniferous|||||||
35080|Elimeek Volcanics|23508|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
35080|Elimeek Volcanics|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Wallaman Falls Volcanics; Janet Ranges, Koolmoon, Silent Creek and Torres Strait Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
28530|Elizabeth Creek Granite|9539|5|Briefly described|Map legend|Carboniferous|Carboniferous|Pink biotite leucogranite; minor porphyritic biotite microgranite, pink aplite, grey greisen.||||||
28530|Elizabeth Creek Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Late Carboniferous|I-type granite. Apatite fission track analyses are detailed.||Unit in O'Brien Supersuite.||||
28530|Elizabeth Creek Granite|22669|6|Mentioned|P259||Namurian|Age of unit is 318 Ma||||||
28530|Elizabeth Creek Granite|22744|6|Mentioned|P12|||||||||
28530|Elizabeth Creek Granite|23291|5|Briefly described|p100 Tb. 3.12|Late Carboniferous|Late Carboniferous|Parent: O'Brien's Creek Suite. Age: 318Ma (Black& Holmes; 315Ma (Champion 1991). Geological Province: Georgetown Region.||||||08-JUL-15
28530|Elizabeth Creek Granite|23429|5|Briefly described|p444|||||||||
28530|Elizabeth Creek Granite|23430|5|Briefly described|Plate 14.7a|||Also see p493. I-type granite.||||||
28530|Elizabeth Creek Granite|23493|5|Briefly described|p9, p19 Tb. 1|Triassic|Permian|Pink to red massive medium- to fine-grained slightly porphyritic granite.  Conformably overlain by Cumbana Rhyolite Porphyry.  Intrudes Newcastle Range Volcanics.||||||
28530|Elizabeth Creek Granite|23494|4|Described|p10, p20 Tb. 1|Triassic|Permian|Unconformably overlain by McBride Basalt.  Grades upwards into Cumbana Rhyolite Porphyry, Tiger Hill Microgranite.||||||
28530|Elizabeth Creek Granite|23498|6|Mentioned|p20 table 1|||||||||
28530|Elizabeth Creek Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
28530|Elizabeth Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No.5. I-Type.||||||
28530|Elizabeth Creek Granite|23619|4|Described|p40 Table 2||Carboniferous|Rb-Sr biotite 318 Ma. Also see p10. Overlain by Undara Basalt. Cumbana Batholith Province.||||||21-OCT-08
28530|Elizabeth Creek Granite|23624|6|Mentioned|p20|||||||||
28530|Elizabeth Creek Granite|23713|6|Mentioned|p46|||Of Ootann Supersuite.||||||
28530|Elizabeth Creek Granite|24013|5|Briefly described|p17 Tb. 1|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
28530|Elizabeth Creek Granite|29605|6|Mentioned|p1|||||||||
28530|Elizabeth Creek Granite|29793|6|Mentioned|Fig.1|||||||||
28530|Elizabeth Creek Granite|29794|6|Mentioned|Fig.1|||||||||
28530|Elizabeth Creek Granite|29795|6|Mentioned|p273|||||||||
28530|Elizabeth Creek Granite|29796|6|Mentioned|p323|||||||||
28530|Elizabeth Creek Granite|29803|6|Mentioned|p557|||||||||
28530|Elizabeth Creek Granite|29814|6|Mentioned|p815|||||||||
28530|Elizabeth Creek Granite|29815|6|Mentioned|p994|||||||||
28530|Elizabeth Creek Granite|29820|6|Mentioned|p450|||||||||
28530|Elizabeth Creek Granite|30505|4|Described|p3|||See also p5-8,14,16. Mid-Carboniferous to Early Permian age.||||||21-OCT-08
28530|Elizabeth Creek Granite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
28530|Elizabeth Creek Granite|31435|6|Mentioned|p8|||||||||
28530|Elizabeth Creek Granite|31453|6|Mentioned|p617|||||||||
28530|Elizabeth Creek Granite|31832|6|Mentioned|Table 6|||||||||
28530|Elizabeth Creek Granite|32360|6|Mentioned|p740|||||||||
28530|Elizabeth Creek Granite|32487|6|Mentioned|p16|||||||||
28530|Elizabeth Creek Granite|32518|6|Mentioned|p769|||||||||
28530|Elizabeth Creek Granite|32528|5|Briefly described|Table 1|||||||||
28530|Elizabeth Creek Granite|32531|6|Mentioned|p478|||||||||
28530|Elizabeth Creek Granite|32553|4|Described|p58|||||||||
28530|Elizabeth Creek Granite|32654|4|Described|p96|||Perm. Refers Richards et al. (1966). Age.||||||
28530|Elizabeth Creek Granite|32655|6|Mentioned|p760|||||||||
28530|Elizabeth Creek Granite|32818|5|Briefly described|p21|||Age & mineralization||||||
28530|Elizabeth Creek Granite|32836|6|Mentioned|p8|||Refers Richards et al. (1966)||||||
28530|Elizabeth Creek Granite|33179|4|Described|Table 1|||||||||
28530|Elizabeth Creek Granite|33180|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28530|Elizabeth Creek Granite|33205|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
28530|Elizabeth Creek Granite|33221|6|Mentioned|p20|||Perm. - Carb.||||||
28530|Elizabeth Creek Granite|33429|6|Mentioned|p1236|||See also Fig.1.||||||
28530|Elizabeth Creek Granite|33430|6|Mentioned|p562|||||||||
28530|Elizabeth Creek Granite|33635|6|Mentioned|Fig.1|||||||||
28530|Elizabeth Creek Granite|33777|4|Described|p30|||||||||
28530|Elizabeth Creek Granite|33909|6|Mentioned|p231|||||||||
28530|Elizabeth Creek Granite|33963|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
28530|Elizabeth Creek Granite|34573|6|Mentioned|p32|||About 300 my.||||||
28530|Elizabeth Creek Granite|34955|6|Mentioned|p227|||||||||
28530|Elizabeth Creek Granite|35000|6|Mentioned|p137|||||||||
28530|Elizabeth Creek Granite|35214|6|Mentioned|p8|||||||||
28530|Elizabeth Creek Granite|35257|6|Mentioned|p173|||||||||
28530|Elizabeth Creek Granite|35434|6|Mentioned|p36|||||||||
28530|Elizabeth Creek Granite|35633|6|Mentioned|p14|||Mineralization||||||
28530|Elizabeth Creek Granite|35946|6|Mentioned|p28|||||||||
28530|Elizabeth Creek Granite|36527|6|Mentioned|p157|||||||||
28530|Elizabeth Creek Granite|36563|6|Mentioned|Table 1|||||||||
28530|Elizabeth Creek Granite|37571|6|Mentioned|p136|||||||||
28530|Elizabeth Creek Granite|37574|6|Mentioned|p194|||||||||
28530|Elizabeth Creek Granite|37575|6|Mentioned|p179|||||||||
28530|Elizabeth Creek Granite|37633|6|Mentioned|Table 36|||||||||
28530|Elizabeth Creek Granite|38225|6|Mentioned|p391|||See also Fig.2.||||||
28530|Elizabeth Creek Granite|38297|5|Briefly described|p327|||||||||
28530|Elizabeth Creek Granite|38688|6|Mentioned|p47|||||||||
28530|Elizabeth Creek Granite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
28530|Elizabeth Creek Granite|39252|5|Briefly described|p16|||||||||
28530|Elizabeth Creek Granite|39278|6|Mentioned|p353|||Tin mineralization. See also P359||||||
28530|Elizabeth Creek Granite|39283|4|Described|p416|||petrology||||||
28530|Elizabeth Creek Granite|39445|5|Briefly described|Table 12|||See mineral deposits p92. See also p90.||||||21-OCT-08
28530|Elizabeth Creek Granite|39564|6|Mentioned|p7|||||||||
28530|Elizabeth Creek Granite|39687|6|Mentioned|p4|||||||||
28530|Elizabeth Creek Granite|39689|6|Mentioned|p58|||||||||
28530|Elizabeth Creek Granite|39831|6|Mentioned|p319|||||||||
28530|Elizabeth Creek Granite|39845|6|Mentioned|p23|||||||||
28530|Elizabeth Creek Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28530|Elizabeth Creek Granite|39998|6|Mentioned|p191|||||||||
28530|Elizabeth Creek Granite|40049|6|Mentioned|Fig.2|||||||||
28530|Elizabeth Creek Granite|40743|5|Briefly described|p311|||||||||
28530|Elizabeth Creek Granite|40918|6|Mentioned|p101|||||||||
28530|Elizabeth Creek Granite|41125|5|Briefly described|p54|||||||||
28530|Elizabeth Creek Granite|41235|6|Mentioned|p40|||||||||
28530|Elizabeth Creek Granite|41272|5|Briefly described|M 1of1 I01|||||||||
28530|Elizabeth Creek Granite|41680|5|Briefly described|p106|||||||||
28530|Elizabeth Creek Granite|42164|6|Mentioned|p86|||||||||
28530|Elizabeth Creek Granite|42189|6|Mentioned|p262|||||||||
28530|Elizabeth Creek Granite|42200|6|Mentioned|Fig.1 P325|||||||||
28530|Elizabeth Creek Granite|42547|4|Described|p75|||||||||
28530|Elizabeth Creek Granite|42681|6|Mentioned|p20|||||||||
28530|Elizabeth Creek Granite|42691|5|Briefly described|map legend|Paleozoic||||||||07-NOV-08
28530|Elizabeth Creek Granite|43087|6|Mentioned|p21|||Of O'Briens Creek Supersuite||||||
28530|Elizabeth Creek Granite|43110|5|Briefly described|p46|||||||||
28530|Elizabeth Creek Granite|43113|4|Described|Table 2 p25||Carboniferous|RB-Sr biotite age of 318 Ma. (Bain & others,in prep)||||||
28530|Elizabeth Creek Granite|43253|5|Briefly described|map legend||Carboniferous|||||||
28530|Elizabeth Creek Granite|43259|4|Described|Appendix 1,p15.||Carboniferous|U-Pb zircon age is 318 Ma.||||||
28530|Elizabeth Creek Granite|43664|6|Mentioned|p96|||||||||
28530|Elizabeth Creek Granite|43716|6|Mentioned|p17,21|||||||||
28530|Elizabeth Creek Granite|43740|4|Described|p17|||||||||
28530|Elizabeth Creek Granite|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
28530|Elizabeth Creek Granite|43898|14|Not recorded|Map Legend|Triassic|Late Permian|||||||
28530|Elizabeth Creek Granite|43901|14|Not recorded|Map Legend||Late Permian|(Early Triassic) - Late Permian||||||
28530|Elizabeth Creek Granite|43904|14|Not recorded|Map Legend||Neoproterozoic|||||||
28530|Elizabeth Creek Granite|43926|14|Not recorded|p17,Tb.2,opp.10|||||||||
28530|Elizabeth Creek Granite|44047|14|Not recorded|Map Legend||Permian|||||||
28530|Elizabeth Creek Granite|44048|14|Not recorded|Map Legend||Permian|(Triassic?)||||||
28530|Elizabeth Creek Granite|44053|2|Defined|p241|||||||||
28530|Elizabeth Creek Granite|44057|14|Not recorded|p606-607|||||||||
28530|Elizabeth Creek Granite|44059|14|Not recorded|p442(Tb.)||Neoproterozoic|||||||
28530|Elizabeth Creek Granite|44258|14|Not recorded|p1,5,7,12-18,25-27,||Neoproterozoic|Average age 280 Ma. p31,35,36,38||||||
28530|Elizabeth Creek Granite|44259|14|Not recorded|p107|||282+-12 Ma||||||
28530|Elizabeth Creek Granite|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
28530|Elizabeth Creek Granite|44425|14|Not recorded|p18,22,opp.11,map|||||||||
28530|Elizabeth Creek Granite|44542|2|Defined|p26||Late Paleozoic|||||||07-NOV-08
28530|Elizabeth Creek Granite|44560|14|Not recorded|p359||Late Carboniferous|||||||
28530|Elizabeth Creek Granite|44586|14|Not recorded|p380||Late Carboniferous|K-Ar:Late Carboniferous.||||||
28530|Elizabeth Creek Granite|44815|14|Not recorded|unknown (p313-346)|||||||||
28530|Elizabeth Creek Granite|44826|14|Not recorded|p39,40|||||||||
28530|Elizabeth Creek Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|321 +/- 4 Ma, SHRIMP||||||
28530|Elizabeth Creek Granite|45003|14|Not recorded|p13,27-8,42|||||||||
28530|Elizabeth Creek Granite|45008|14|Not recorded|p12,39-43,51,95,109|||maps.||||||
28530|Elizabeth Creek Granite|45009|14|Not recorded|p21,75,110,111,131,||Permian|Tb.13,Pl.13. Intrudes Herbert River Granite and Newcastle Range Volcanics.||||||
28530|Elizabeth Creek Granite|45014|2|Defined|p43-5,80-5,99-110,|Early Permian|Early Carboniferous|(Middle Carboniferous-Early Permian)||||||
28530|Elizabeth Creek Granite|45025|4|Described|p75-6,anal.p82-3|Permian|Carboniferous|||||||
28530|Elizabeth Creek Granite|45065|4|Described|Table 4|||||||||
28530|Elizabeth Creek Granite|45086|5|Briefly described|p45|||Permian - Carb.||||||
28530|Elizabeth Creek Granite|45087|6|Mentioned|p9|||Chemical analyses.||||||
28530|Elizabeth Creek Granite|45113|3|Fully described|p11|||Emphasis on petrography. Also mentioned p9.||||||21-OCT-08
28530|Elizabeth Creek Granite|46845|6|Mentioned|p138|||||||||
28530|Elizabeth Creek Granite|46879|6|Mentioned|p174|||||||||
28530|Elizabeth Creek Granite|48745|6|Mentioned|p115|||||||||
28530|Elizabeth Creek Granite|48894|6|Mentioned|p47|||See also PP53,54. 315my.||||||
28530|Elizabeth Creek Granite|48976|4|Described|p10|||Isotopic data Table 2||||||
28530|Elizabeth Creek Granite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
28530|Elizabeth Creek Granite|60081|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink massive leucocratic adamellite.||||||
28530|Elizabeth Creek Granite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Biotite granite, microgranite.||||||
28530|Elizabeth Creek Granite|60425|6|Mentioned|p181|||Of de Keyser (1961). Now part of Almaden Supersuite - name probably obsolete therefore?||||||07-FEB-11
28530|Elizabeth Creek Granite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. High K, Th and U radiometrric responses.|||||Mainly pink, medium- to coarse-grained, even-grained to seriate biotite granite; minor porphyritic biotite granite and microgranite.|
28530|Elizabeth Creek Granite|68405|5|Briefly described|Map Legend|Bashkirian|Bashkirian|Kennedy Province. Late Carboniferous age, SHRIMP dated. Altered biotite to porphyritic biotite granite occur in both subdivisions.|321 +/- 4 Ma|Of the O'Briens Creek Supersuite. |Informally subdivided into two units.||Fine to coarse-grained, porphyritic to locally even-grained biotite granite, locally altered; mainly pink, medium to coarse-grained, even-grained to seriate biotite granite with minor porphyritic biotite granite and microgranite, locally altered.|
28530|Elizabeth Creek Granite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Mainly pink, medium to coarse-grained, even-grained to seriate biotite granite; minor porphyritic biotite granite and microgranite.|
28530|Elizabeth Creek Granite|69593|4|Described|p484, p486, p487 Fig.6.9, p510|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Forms bouldery outcrops. Sm-Nd isotope data tabulated.|321 +/- 4 Ma.|O'Briens Creek Supersuite.||Is intruded by O'Briens Creek Microgranite.|I-type.|
28530|Elizabeth Creek Granite|72297|5|Briefly described|p757, p759|Carboniferous|Carboniferous|O'Brien's Creek gemfield, near Mount Surprise.  Gems occur in alluvial gravels and colluvial hill wash.|||||Includes quartz-pegmatite dykes, veins and segregations containing gem-quality topaz, beryl and aquamarine.|
80378|Elizabeth Sandstone|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT).||Accident Subgroup.||Unconformably overlies Constance Sandstone. Is overlain by Mullera Formation.||
80378|Elizabeth Sandstone|71369|3|Fully described|p6-7, p12, p23, p32-38, p44, p48-50|Mesoproterozoic|Mesoproterozoic|New name in this study (Sweet, 2017) for sandstones overlying Bowthorn Member and underlying Mullera Formation. Previously mapped as an unnamed component of Constance Sandstone; separated following recognition of an unconformity. The type section is ~20km SSE of Bowthorn homestead. Its stratigraphic span had not been included in the original type section of the Constance Sandstone by Carter et al. (1961). South Nicholson Basin. Mapped as Constance Sandstone in NT. Appears as Elizabeth Sandstone Member on p28. c.200m thick. Transgressive deposits.||Accident Subgroup.||Unconformably overlies Bowthorn Member (Constance Sandstone). Is overlain conformably by Mullera Formation.|Thick-bedded, large-scale trough cross-bedded, coarse- to very coarse- and granule-rich sandstone; the upper part is marginally finer-grained and better sorted.|
80378|Elizabeth Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich quartzose sandstone.|
80378|Elizabeth Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.||Overlain by Mullera Formation. vUnderlain unconformably by Constance Sandstone.|Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich quartzose sandstone.|
80378|Elizabeth Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Accident Subgroup.||Overlain by Mullera Formation. vUnderlain unconformably by Constance Sandstone.|Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich quartzose sandstone.|
80378|Elizabeth Sandstone|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich quartzose sandstone.|
80378|Elizabeth Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich, quartzose sandstone|
80378|Elizabeth Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich, quartzose sandstone|
80378|Elizabeth Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich, quartzose sandstone|
80378|Elizabeth Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|||Thick-bedded, trough cross-bedded, coarse to very coarse-grained and granule-rich, quartzose sandstone|
80378|Elizabeth Sandstone|72526|5|Briefly described|p33-34, p40, p46.|||Of Sweet, 2017. Part of original Constance Sandstone above the unconformity in Qld.||||Overlies Constance Sandstone in Queensland.||
80378|Elizabeth Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Only recognised in Qld.||Accident Subgroup, South Nicholson Group||Overlain by Mullera Formation.||
80378|Elizabeth Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Partial aquifer.||Accident Subgroup, South Nicholson Group||Unconformably underlain by the Constance Sandstone, including the Bowthorn Member. Overlain by Mullera Formation.||
79970|Ella Granite|71965|5|Briefly described|p910-911,913|||Geological province: Thomson Orogen. Of the Ella Belt. Intersected in drillhole DIO Ella 1. Dated at 425.4+\-6.6 Ma (Cross et al., 2018).|425.4+\-6.6 Ma|||||
79970|Ella Granite|71966|5|Briefly described|p991,996|Ludlow|Ludlow|Geological province:  Thomson Orogen. S-type granite, part of a batholithic scale belt of intrusions termed the Ella belt (Purdy et al., 2018). Intersected in drillhole DIO Ella 1, and samples analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 1586685 yielded 206Pb/238U age of 425.4+\-6.6 Ma, interpreted as crystallisation age.|425.4+\-6.6 Ma (crystallisation)|||||
79970|Ella Granite|72522|5|Briefly described|p70, p78.|Late Silurian|Late Silurian|Located within the Ella Belt south of GSQ Thargomindah.|c. 419-425 Ma|||||
79970|Ella Granite|72951|6|Mentioned|p1026, 1028|Silurian|Silurian|Thomson Orogen, southern. S-type granite.|425.4 +/- 6.6 Ma|||||
80010|Ellen Harkins carbonaceous shale|70913|3|Fully described|p8 fig 3, p9, p56-p57|Middle Permian|Early Permian|Gympie Province. Informal name [of Bed rank, intended to be replaced by the formal Ellen Harkins Shale Bed]. This unit, though minor, is named because of its importance as a source of gold in historic times as part of the 'third bed of slate'. Name derived from the Ellen Harkins Mine, near Deep Creek, Gympie. See also Ellen Harkins beds p45, Ellen Harkins shale p44, 56, 67, 87, Ellen Harkins Shale bed p11 and Ellen Harkins Shale Member,inferred from p8 Fig 3 . One drill hole contains intermittent fractured layers of this unit. Mostly 5-10m thick but may be up to 200m thick in some areas. Distribution briefly discussed. Occurs intermittently throughout the siltstone facies of the Dawn Formation. Reference section in GEGM drill hole G215 stored at Zillmere core library.||Dawn Formation|||A reduced facies of tuffaceous shale or siltstone.|27-FEB-19
36482|Ellendale granite|23291|4|Described|p89 Fig. 3.8|||Informal name. Of the White Springs Supersuite. Geological Province: Georgetown Region.||||||21-OCT-08
36482|Ellendale granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 54  Assumed to be I-Type.||||||
36482|Ellendale granite|69592|5|Briefly described|p282|Silurian|Silurian|Champion and Heinemann (1994). Informal name.||White Springs Supersuite.|||I-type.|
28142|Ellenvale beds|23422|4|Described|p183, p204 Table 6.3|Early Permian|Carboniferous|Also referred to as Ellenvale Beds.  Maximum thickness: >3000m.||||||
28142|Ellenvale beds|23430|5|Briefly described|p504 Table 14.5|||Underlying Unit Horse Pocket Volcanics - unconformable.||||||
28142|Ellenvale beds|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
28142|Ellenvale beds|23893|5|Briefly described|p19|Early Permian|Late Carboniferous|||||||
28142|Ellenvale beds|24612|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|Geological Province: Burdekin Basin.||||||
28142|Ellenvale beds|24613|5|Briefly described|p6 Fig. 3, p92-94|Early Devonian|Precambrian|Once mapped with Glenrock Group, are now excluded from this grouping. Unconformably overlie Mount Douglas Formation and Percy Creek Volcanics. Geological province: Burdekin Basin. Also written as Ellenvale Beds (p113, p114).||||||07-FEB-11
28142|Ellenvale beds|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
28142|Ellenvale beds|42295|5|Briefly described|Fig.2 P5|||||||||
28142|Ellenvale beds|43095|6|Mentioned|p28|||of Glenrock Group? NO||||||
28142|Ellenvale beds|65706|4|Described|p14 Tbl.1,|Carboniferous|Carboniferous|Fault controlled.|||||Rhyolitic lavas and volcaniclastics, rhyolite breccia, andesite, subgreywacke, feldspathic sandstone, conglomerate, shale, mudstone.|
28142|Ellenvale beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Balfes Creek and Wade beds; Insolvency Gully and Marshs Creek Formations; and Silver Valley Conglomerate, are all mapped under the symbol, CPs.||||||
28142|Ellenvale beds|68576|5|Briefly described|Q_11: p43|||Reid River area.|||||Layered silicic volcanics.|
28142|Ellenvale beds|68731|5|Briefly described|p204|Pennsylvanian|Pennsylvanian|Wyatt et al. (1970); Wyatt and Jell (1980). Lies centrally in MINGELLA, occupying the Reid River Graben. ~ 3000 m thick. Age constrained by the underlying Mississippian Horse Pocket Volcanics.||||Unconformably underlain by the Horse Pocket Volcanics.|Comprises rhyolitic flows and pyroclastics, volcaniclastic sandstone, volcanic breccia, conglomerate, shale and mudstone.|03-JUL-14
28142|Ellenvale beds|69593|5|Briefly described|p495|Permian|Late Carboniferous|Younger age may be Late Carboniferous.|||||Crystal-rich rhyolitic ignimbrite, rhyolite lava, volcaniclastic and epiclastic rocks, and other sediments; minor mafic rocks.|
81097|Elliot River Granodiorite|69594|6|Mentioned|p567 Fig.7.39|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.||||||
81097|Elliot River Granodiorite|73029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Pale pink, grey or pale greyish pink, fine to medium-grained, porphyritic hornblende-biotite, biotite-hornblende, and biotite granodiorite to monzogranite; traces of titanite and scattered mafic inclusions to c. 3 cm; cut by mafic dykes.|
37021|Elliott Surface|23251|5|Briefly described|p3, p26|||Named by Grimes (1992). Occur to the east of the Como Scarp. An indurated landscape. Geological Province:  Maryborough Basin.||||||21-JUN-06
37021|Elliott Surface|63821|4|Described|p10-11|||Of Grimes (1991). Preserved on cliff-forming sst of Tertiary Elliot Fm in NW of MARYBORO' sheet; lateritised Terti.+ Cret.formations in SE corner. Overlies Booyal Surface N. of Gregory River and S.of Mary River. Duricrust (mainly ferricrete) soil profile||||||07-FEB-11
37021|Elliott Surface|69599|5|Briefly described|p584, p586|Miocene|Oligocene|Bundaberg area; Maryborough Basin. Silcrete and ferruginisation, with the latter continuing into Miocene.||||||
38893|Ellrott Rhyolite|24420|5|Briefly described|p7|Early Permian|Early Permian|Of Berserker Group.||||||
38893|Ellrott Rhyolite|24615|5|Briefly described|CD|Permian|Permian|[Pkr].  Intrusive porphyritic rhyolite and dacite, possibly locally extrusive lava and breccia.||||||
38893|Ellrott Rhyolite|50207|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||
38893|Ellrott Rhyolite|50208|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||
38893|Ellrott Rhyolite|50209|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||17-MAY-04
38893|Ellrott Rhyolite|50212|5|Briefly described|Map Legend|Permian|Permian|Of Berserker Group||||||
38893|Ellrott Rhyolite|60557|5|Briefly described|p25|||Rhyolitic to dacitic volcanic domes, some of which may be extrusive.||||||09-JUN-05
38893|Ellrott Rhyolite|61778|3|Fully described|p233, p234 Fig. 1, p236, p240 Fig. 11||Early Permian|Of Berserker Group. Age: 276+/-4 and 268+/-4Ma. Consists of felsic to intermediate intrusive and extrusive volcanic domes. Geological Province: Berserker Subprovince. See p236 for detailed lithology.||||||07-FEB-11
38893|Ellrott Rhyolite|64429|2|Defined|p15, p22|Early Permian|Early Permian|Widespread within Berserker Group. Previously called Ellrott Ryolites (Taube 1979). This unit is a likely source of Sleipner Member. Comprises rhyolite and dacite volcanic domes (intrusive) and some rock is extrusive - detailed lithology included.||||||04-SEP-08
38893|Ellrott Rhyolite|68008|3|Fully described|p158-160, p162, p164, p166, p169-170|Permian|Permian|See also p307, p484, p527. Originally Ellrott Rhyolites of Taube (1979). Published as Ellrott Rhyolite by Hunns (1994). Part of the Berserker Series (Whitehouse, 1930), renamed the Berserker beds (Kirkegaard et al., 1970), which was divided into the Berserker Group (Crouch and Parfrey, 1998) including this unit. The type area is Cabbage Tree Hill. Coeval with upper half of Chalmers Formation. Geochemistry described. U-Pb zircon ages (Fanning, 2012). Source of Sleipner Member.|276 +/- 3.9 Ma; 268.2 +/- 3.9 Ma.|Berserker Group.||Intrudes Lakes Creek Formation and Sleipner Member (Chalmers Formation).|Domes of rhyolite to dacite (occasionally andesite); massive or flow-banded, porphyritic, amygdaloidal, local xenoliths. Many are adjacent to monomict breccia; a local ?peperite.|
38893|Ellrott Rhyolite|68679|5|Briefly described|p350|||Taube (1979), Hunns (1994). Berserker Subprovince, Yarrol Province. Occurs as widespread volcanic domes, some of which may be extrusive, up to several km2 in area. Many have brecciated margins and peperitic contacts.||Berserker Group.|||Rhyolite, dacite and possibly andesite; typically massive with plagioclase and K-feldspar phenocrysts; visible quartz is rare; groundmass is microcrystalline and devitrified; some flow-banded rocks are autobrecciated; amygdales common.|
38893|Ellrott Rhyolite|71592|5|Briefly described|Appendix A.|||New England Orogen.|276+/-3.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite, rhyolite.|
36427|Elphinstone Granite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|I-Type. Also see p26-27. Proposed type area is north-west foothills of Mount Slopeway (8161-3957 79588). Kennedy Province.||||||
36427|Elphinstone Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36427|Elphinstone Granite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
36394|Elphistone Creek Gabbro|23429|5|Briefly described|Fig 13.25(b)|||||||||
78922|Elvinia Member|65388|4|Described|p160, 162, 165|Artinskian|Artinskian|Upper siltstone of Buffel Formation. ~55m thick and consists mainly of fossiliferous silty to sandy limestone grading upwards into recessive calcareous siltstone in cycles 3-10m thick. May be disconformable on Dresden Limestone Member.||||||
29984|Emerald Creek Microgranite|23423|5|Briefly described|p311 Table 7.4|Early Permian|Late Carboniferous|Also see p245. Emerald Creek Supersuite.||||||
29984|Emerald Creek Microgranite|23497|5|Briefly described|Table 1|Early Permian|Late Carboniferous|of Emerald Creek Supersuite, Kennedy Province. Intrudes Hodgkinson Formation rocks and is cut by the Tinaroo Granite. Age: ~320Ma.||||||
29984|Emerald Creek Microgranite|23506|5|Briefly described|Map Legend|Permian|Carboniferous|of Emerald Creek Supersuite.||||||
29984|Emerald Creek Microgranite|23507|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
29984|Emerald Creek Microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 391. S-Type.||||||
29984|Emerald Creek Microgranite|23616|4|Described|p79||Carboniferous|Intruded by Tinaroo Granite. Of Emerald Creek Supersuite. Hodgkinson Province.||||||
29984|Emerald Creek Microgranite|43060|5|Briefly described|p110|||Of Emerald Creek Supersuite. Age no older than Middle Carboniferous.||||||
29984|Emerald Creek Microgranite|43259|4|Described|Appendix 1,p44.||Carboniferous|U-Pb zircon age is 320+/-6 Ma. Carboniferous?,possibly Permian.||||||
29984|Emerald Creek Microgranite|60425|3|Fully described|p56-57 Tb. 4, p181|Early Permian|Late Carboniferous|Of the Emerald Creek Supersuite. Intruded Hodgkinson Formation; cut by Tinaroo Granite.  Part of the Tinaroo Batholith. Detailed lithology included for this muscovite-biotite granite. S-type||||||07-FEB-11
29984|Emerald Creek Microgranite|62371|5|Briefly described|p472 Fig.3|Early Carboniferous||Age: 348+/-6 Ma (Zuchetto et al., 1999)||||||09-JUN-06
29984|Emerald Creek Microgranite|63140|5|Briefly described|p572 fig 3|Early Carboniferous|Late Devonian||348 +/- 6 Ma (Zucchetto et al. 1999).|||||
29984|Emerald Creek Microgranite|63154|5|Briefly described|p281 Fig. 3|Early Carboniferous|Early Carboniferous|Age: ~350Ma. Geological province: Hodgkinson Province. Associated gold mineralisation.||||||11-APR-07
29984|Emerald Creek Microgranite|69592|4|Described|p242, p298|Mississippian|Mississippian|Douglas Creek area. Distinguished by relatively high MgO and CaO, and low K2O. Has gently-dipping contacts and a wide (up to 10km across) contact metamorphic aureole. Syn-tectonic emplacement.|347 +/- 6.4 Ma (SHRIMP; Zucchetto et al., 1999).|Emerald Creek Supersuite.||Abuts (and is partly stoped out by) Tinaroo Granite.|Two-mica microgranite; migmatite developed locally close to contact with country-rock.|
29984|Emerald Creek Microgranite|70207|5|Briefly described|p5, p11, p45-51|||Douglas Creek area. Unit of the Kennedy Igneous Association. Post-tectonic. Previously dated at ~320 +/- 6 Ma (reported by Bultitude and Champion, 1992) and 347.5 +/- 6.4 Ma (Zucchetto, 1999) and interpreted as syn-tectonic.|328.2 +/- 2.5 Ma (Kositcin et al., 2015).|||Intrudes Hodgkinson Formation.|S-type. Pale grey, medium-grained, essentially even-grained biotite-muscovite monzogranite. Appears little deformed in outcrop, but quartz grains invariably show undulose extinction.|
29984|Emerald Creek Microgranite|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen.|328+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
29984|Emerald Creek Microgranite|72983|6|Mentioned|p22|Serpukhovian|Serpukhovian|Date from Kositcin et al. (2015).|328.2 +/- 2.5 Ma|||||
36711|Emerald Creek Suite|23423|5|Briefly described|p311 Table 7.4|Early Permian|Carboniferous|Of Emerald Creek Supersuite.||||||
36711|Emerald Creek Suite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit , as well as the Almaden, Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||06-JUN-13
29983|Emerald Creek Supersuite|23423|4|Described|p311 Table 7.4|Early Permian|Late Carboniferous|Age: ~320 +/- 6 Ma. Intrudes Hodgkinson Formation. Also see p245.||||||
29983|Emerald Creek Supersuite|23430|6|Mentioned|p493|||||||||
29983|Emerald Creek Supersuite|23497|6|Mentioned|p34|||||||||
29983|Emerald Creek Supersuite|23506|5|Briefly described|Map Legend|Permian|Carboniferous|Contains Emerald Creek Microgranite.||||||
29983|Emerald Creek Supersuite|23616|4|Described|p79||Carboniferous|Comprised of one unit: Emerald Creek Microgranite. In the Hodgkinson Province.||||||22-APR-09
29983|Emerald Creek Supersuite|43060|4|Described|p110|||||||||
29983|Emerald Creek Supersuite|44246|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|(Middle Carboniferous - Late Carboniferous)||||||
29983|Emerald Creek Supersuite|60425|3|Fully described|p56 Tb. 4, p79|Early Permian|Late Carboniferous|Comprises just Emerald Creek Microgranite. Intruded Hodgkinson Formation; cut by Tinaroo Granite. Part of the Tinaroo Batholith. Detailed lithology presented for this supersuite. S-type.||||||07-FEB-11
29983|Emerald Creek Supersuite|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.|347 +/- 6.4 Ma (SHRIMP).||||S-type granitoids.|
29983|Emerald Creek Supersuite|69592|5|Briefly described|p242|Mississippian|Mississippian|Bultitude and Champion (1992).|||Emerald Creek Microgranite.|||
80897|Emerson Gap Granite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.|Ootann Supersuite.||||
80921|Emma Creek Tonalite|69592|6|Mentioned|p283|Silurian|Silurian|||Dido Supersuite.||||
23580|Emu Mill Granodiorite|22847|3|Fully described|p 50|Early Devonian|Late Silurian|||||||
23580|Emu Mill Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23580|Emu Mill Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23580|Emu Mill Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 120. I-Type.||||||
23580|Emu Mill Granodiorite|42245|2|Defined|p37|Early Devonian|Late Silurian|||||||
23580|Emu Mill Granodiorite|42633|6|Mentioned|Table 1 P8|||||||||
23580|Emu Mill Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23580|Emu Mill Granodiorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|||||||
23580|Emu Mill Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23580|Emu Mill Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23580|Emu Mill Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Emu Mill gdrt.||Unit in Millchester Supersuite.||||
80673|Emu Yard Granite|71849|3|Fully described|p3, p5, p8, p15, p91-94, p121-122, p150|Devonian|Devonian|See also p158, p160-161, p184, p195. New name, after Emu Yard ~4km NW of the type area at MGA 717016 8478402. Previously mapped as part of Kintore Adamellite. Coen Inlier. Small, NW-aligned elongate pluton ~14km W of Coen. Deeply weathered, poorly exposed, mainly as scattered boulders and tors. Geophysics briefly described; lithology and geochemistry detailed.||Lankelly Suite.||Inferred to intrude Yarraden Schist. Is overlain nonconformably by Falloch beds.|Shoshonitic, peraluminous S-type. Grey, fine- to medium-grained, slightly porphyritic biotite-muscovite and muscovite-biotite monzogranite. Minor to trace garnet, rare sillimanite and altered cordierite. Extensively deformed and recrystallised.|
80673|Emu Yard Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Lankelly Suite.|||Grey, fine- to medium-grained, slightly porphyritic biotite-muscovite and muscovite-biotite monzogranite; extensively deformed and recrystallised; muscovite the dominant mica locally.|
23581|Emuford Granite|23423|5|Briefly described|p314 table 7.4|||Intruded by Gurrumba Ring Complex. O'Briens Creek Supersuite.||||||
23581|Emuford Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~313-315 Ma. of O'Briens Creek Supersuite.||||||
23581|Emuford Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||01-JUN-09
23581|Emuford Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite. Age: 313 - 315Ma.||||||01-JUN-09
23581|Emuford Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite. Age ~317+/-2Ma Rb-Sr.||||||01-JUN-09
23581|Emuford Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 263.  I-Type.||||||
23581|Emuford Granite|23616|6|Mentioned|p41|||See also p75. Of O'Briens Creek Supersuite.||||||
23581|Emuford Granite|23624|4|Described|p20|||Of O'Brien's Creek Supersuite.||||||29-APR-09
23581|Emuford Granite|39283|4|Described|p419|||||||||
23581|Emuford Granite|39997|6|Mentioned|p165|||||||||
23581|Emuford Granite|41235|4|Described|p42|||||||||
23581|Emuford Granite|43060|5|Briefly described|p61,101|||Of O'Briens Creek Supersuite.||||||01-JUN-09
23581|Emuford Granite|43259|4|Described|Appendix 1,p34.||Carboniferous|||||||
23581|Emuford Granite|60425|4|Described|p61 Tb. 4, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Intruded by rocks of the Gurrumba Ring Complex. Recent mapping included Black Diamond and Reids Granite in this biotite granite. Detailed lithology given; I-type. Informally referred to as Emu Granite.||||||07-FEB-11
23581|Emuford Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Mapped separately are two geophysical subdivisions, both of uncertain rock type but both said to be "probably variants" of this unit's lithology.||Unit in O'Briens Creek Supersuite.|||Pink to cream, coarse-grained, seriate biotite syenogranite and monzogranite, minor fine-grained biotite syenogranite to monzogranite.|
23581|Emuford Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Mapped separately are two geophysical subdivisions, both of uncertain rock type but both said to be "probably variants" of this unit's lithology.||Unit in O'Briens Creek Supersuite.|||Pink to cream, coarse-grained, seriate biotite syenogranite and monzogranite, minor fine-grained biotite syenogranite to monzogranite.|
23581|Emuford Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. High K, Th and U radiometric responses.||Unit in O'Briens Creek Supersuite.|||Pink to cream, coarse-grained, seriate (fluorite)-biotite syenogranite; extensively altered in places; subordinate fine-grained biotite syenogranite.|
23581|Emuford Granite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.|||I-type.|
23581|Emuford Granite|72297|6|Mentioned|p758|||||||||
36212|Emysland Granodiorite|23422|5|Briefly described|p181, p218 Table 6.12|||Of Leichhardt Supersuite.||||||
36212|Emysland Granodiorite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
36212|Emysland Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 81. I-Type.||||||
36212|Emysland Granodiorite|24613|5|Briefly described|p95, p99|||Partially intrudes Mount Douglas Formation on eastern flank. Flow-banded rhyolite dykes associated with Percy Creek Volcanics are probably related to this unit.||||||07-FEB-11
36212|Emysland Granodiorite|43933|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36212|Emysland Granodiorite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36212|Emysland Granodiorite|68419|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Kennedy Province. Minimum age shown as Early Permian.|||||White and pink to grey, slightly porphyritic, hornblende-biotite and biotite granodiorite and biotite granite.|
36212|Emysland Granodiorite|68420|5|Briefly described|Map Legend|Early Permian|Carboniferous|Of the Kennedy Province. |||||White and pink to grey, slightly porphyritic, hornblende-biotite and biotite granodiorite and biotite granite.|
36212|Emysland Granodiorite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|||Slightly porphyritic, hornblende-biotite and biotite granodiorite.|
27148|Endeavour Strait Ignimbrite|23421|4|Described|Table 5.3 p164.||Late Carboniferous|of Torres Strait Volcanic Group. Thickness: +100m. Intruded by Badu Suite.||||||
27148|Endeavour Strait Ignimbrite|23431|6|Mentioned|p537|||||||||
27148|Endeavour Strait Ignimbrite|30916|6|Mentioned|p94|||||||||
27148|Endeavour Strait Ignimbrite|32564|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
27148|Endeavour Strait Ignimbrite|33880|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27148|Endeavour Strait Ignimbrite|33883|6|Mentioned|p9|||||||||
27148|Endeavour Strait Ignimbrite|34582|2|Defined|Table 1|Permian|Carboniferous|Carboniferous - Permian||||||
27148|Endeavour Strait Ignimbrite|43567|5|Briefly described|p402|||||||||
27148|Endeavour Strait Ignimbrite|45076|4|Described|p37|||? Carb.  See also P102.||||||
27148|Endeavour Strait Ignimbrite|71031|5|Briefly described|p2-p3, p38-p39, p41, p43|Early Carboniferous|Early Carboniferous|Oriomo Province. Exposed in a steep cliff above the Punsand Bay beach.||Torres Strait Volcanic Group||Intruded by the Torres Strait Volcanic Group. Overlies the Eborac Ignimbrite.||
27148|Endeavour Strait Ignimbrite|72983|4|Described|p4-5, p7, p61-65|Visean|Tournaisian|Jardine Subprovince, Kennedy Igneous Association. Cape York region. Age is consistent with a previously reported magmatic age of 353.4 +/- 2 Ma from a feldspar-quartz porphyry dyke at the approx. contact with the underlying Eborac Ignimbrite.|349.2 +/- 3.1 Ma SHRIMP U-Pb|Torres Strait Volcanic Group, Badu Supersuite||Underlain by the Eborac Ignimbrite.|Highly silicified, coarse, crystal-rich and locally mineralised (Sn, W) rhyolitic ignimbrite.|
78923|Epsom Granodiorite|65388|2|Defined|p367, p135 Fig. 53, p362, 364, 365, 383|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Deeply weathered, poorly exposed. Is enclosed by and post-dates the Mount Spencer Granodiorite. Likely to post-date Strathdee Granodiorite. Likely one of the youngest units in southern Urannah Batholith.  Probable age given. Dominantly pale grey to pinkish grey, medium to fine-grained, uneven-grained biotite-hornblende granodiorite.||||||
38890|Erebus beds|24420|5|Briefly described|p6|Middle Devonian|Late Silurian|||||||
38890|Erebus beds|24615|5|Briefly described|CD|Devonian|Silurian|[SDe].  Dacitic to rhyolitic volcaniclastic sandstone and conglomerate, minor siltstone, fossiliferous limestone and marble.||||||
38890|Erebus beds|50207|5|Briefly described|Map Legend|Early Devonian|Early Silurian|||||||
38890|Erebus beds|50208|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
38890|Erebus beds|61035|6|Mentioned|p12|Early Devonian|Early Devonian|Informal name. Geological Province: Yarrol Province.||||||07-FEB-11
38890|Erebus beds|61147|5|Briefly described|p376.|||Partly time-equivalent to Craigilee beds. Limestone olistoliths occur at Deversoir.||Unit in Mount Holly Formation.|||Sandstone, siltstone, conglomerate; dacitic and andesitic volcanic rocks; minor autochthonous limestone.|
38890|Erebus beds|61730|5|Briefly described|p994 Fig.1|Middle Devonian|Late Silurian|Previously part of the Mount Holly beds which are now interpreted to be younger. Consists mainly of conglomerate and coarse sandstone sourced from rhyolites, with minor limestone and rare primary volcanic rock. Geol Prov: Yarrol Province. See also p1000.||||||
38890|Erebus beds|63600|5|Briefly described|p900 Fig. 1, p915|Middle Devonian|Late Silurian|||||||07-FEB-11
38890|Erebus beds|68008|2|Defined|p1, p18, p20, p22-26, p38, p85, p89,p113|Early Devonian|Late Silurian|See also p275, p395, p477-478, p488, p568-569, p573, p575, p581-582, p600. Previously mapped as part of the Mount Holly beds (Kirkegaard et al., 1970). Named after Mount Erebus. No type section; a type area is between GR282306 7355986 and GR280906 7356086. Forms a belt of rocks trending SE from Raglan to Catfish Creek. Forms hilly country. Distinctive airborne geophysical characteristics. Geochemistry described. Thickness unknown: neither base nor top exposed; estimated c.2600m. Folded, faulted and strongly cleaved. Coral species listed. Limestone is mined for cement production. Micropaleontology table. Time-equivalent of Craigilee, Calliope beds and Capella Creek Group.||||Intercalated with (fault slices of), unconformably overlies, and thrust over (locally under) Mount Alma Formation. Is overlain by Casuarina beds. Is intruded by Bajool Quartz Diorite. See Comments.|Marine deposits: sandstone, conglomerate, breccia; minor limestone; rare siltstone and rhyolite. Details elaborated in text.|
38890|Erebus beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Marble Waterhole, Craigilee, Calliope, Munbooree and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
38890|Erebus beds|68679|5|Briefly described|p312-314, p338, p340, p347, p425|Devonian|Late Silurian|Northern New England Orogen. Previously part of the (now abandoned) Mount Holly beds (Murray et al., 2012). Is partly coeval with the Calliope beds. The limestones have crinoids, corals, stromatoporoids and brachiopods suspended in micrite. The unit is folded, faulted and strongly cleaved. Corals indicate Emsian age.||||Is thrust (to the W) over Mount Alma Formation. Is intruded by Bajool Quartz Diorite.|Volcaniclastic sandstone, clast-supported granule to cobble conglomerates and breccias; minor limestone variably recrystallised to marble; rare siltstone, dacite and rhyolite lavas or high-level intrusions, commonly quartz or feldspar phyric.|
38890|Erebus beds|73143|6|Mentioned|p11, p18|Emsian|Emsian|Yarrol Basin. Contains Favosites grandipora tabulate coral and Aphyllum simplexum rugose coral (Blake, 2010).||||||
36291|Eresby Volcanics|23291|4|Described|p93 Tb. 3.9|Late Carboniferous|Late Carboniferous|Parent: Scardons Volcanic Group. Age: 289+/-2Ma. Thickness: At least 150m. Geological Province: Georgetown Region.||||||08-JUL-15
36291|Eresby Volcanics|23510|5|Briefly described|Map Legend||Early Permian|||||||
75657|Ernest Creek Granodiorite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Grey, fine to medium-grained biotite-hornblende granodiorite to tonalite; generally moderately to strongly foliated, and with numerous mafic inclusions; traces of titanite and/or allanite present locally.|
39852|Ernest Henry Diorite|24253|5|Briefly described|p9|Proterozoic|Proterozoic|Age: ca. 1660 Ma. Geological Province: Mount Isa Block.||||||
39852|Ernest Henry Diorite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
39852|Ernest Henry Diorite|60665|6|Mentioned|p1153 Fig.5, p1162 Fig.11. |||Summary triangular diagrams for albitization.||||||
39852|Ernest Henry Diorite|61933|6|Mentioned|p169 Fig.3|Paleoproterozoic|Paleoproterozoic|Mentioned in legend only. Age: 1675-1655 Ma. See also p172 Fig.2.||||||07-NOV-08
39852|Ernest Henry Diorite|64248|6|Mentioned|p33 Fig.1, p38 Fig.5, p40 Fig.6 |Statherian|Statherian|See also p41 Tb. 2, p43.|1660 +/- 13 Ma to 1657 +/- 7 Ma.|||||
39852|Ernest Henry Diorite|64250|6|Mentioned|p10 fig 2, p23 fig 8, p11 fig 3, p21|||Cloncurry Fold Belt, Mount Isa Inlier.|1660+/-10 Ma; 1657+/-7 Ma.|||||
39852|Ernest Henry Diorite|64251|6|Mentioned|p51 Fig. 1|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
39852|Ernest Henry Diorite|65396|6|Mentioned|p4, p7, p23, p79, p82, p84-88, p97-98|Statherian|Statherian|See also p161, p173, p175, p179, p183, p193, p195, p199, p213, p234-241, p272, p319, p338-339, p440. Eastern succession, Cloncurry Fold Belt. Appears as Ernest Henry diorite on p85-88. Whole-rock geochemistry detailed. Formations with detrital zircons from this unit are listed.|1660 +/- 13 Ma, 1657 +/- 7 Ma|||||
39852|Ernest Henry Diorite|65755|6|Mentioned|p3 Fig.1|||||||||
39852|Ernest Henry Diorite|66913|5|Briefly described|p171 fig 2|Statharian|Statherian|U-Pb zircon SHRIMP ages and U-Pb titanite TIMS/SHRIMP ages shown diagramatically on Fig. 2.||||||
39852|Ernest Henry Diorite|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||Canobie Domain, Mount Isa Inlier.|1657 +/- 7 Ma.|||||
39852|Ernest Henry Diorite|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1657 +/- 7 Ma.|||||
39852|Ernest Henry Diorite|69591|5|Briefly described|p59|||Sybella Batholith.|1657 +/- 7 Ma (Pollard and McNaughton, 1997).||||Diorite.|
39852|Ernest Henry Diorite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1658+/-10 Ma (U-Pb zircon SHRIMP)||||Diorite.|
39852|Ernest Henry Diorite|73413|6|Mentioned|p3|Statherian|Statherian|Mount Isa Inlier, Eastern Fold Belt.|1657 +/- 7 Ma|||||
39852|Ernest Henry Diorite|73481|6|Mentioned|p441|Statherian|Statherian|Mount Isa Inlier, eastern part.|1670-1650 Ma|||||
39098|Eskdale Igneous Complex|23799|3|Fully described|p85, p116|Triassic|Triassic|Supersedes Eskdale Granodiorite.  Main body intrudes the Maronghi Creek beds, Sugarloaf Metamorphics and Cressbrook Group; intruded by the Crows Nest Granite.  Geological Province: Yarraman Subprovince.||||||
39098|Eskdale Igneous Complex|24560|6|Mentioned|Map legend|||[Located in caption for Magnetic Image - second picture].||||||
39098|Eskdale Igneous Complex|68679|5|Briefly described|p411-415|Middle Triassic|Early Triassic|West of the Esk Basin, northern New England Orogen. Comprises multiple, overlapping zoned plutons, each up to 15km in diameter, defined on magnetic images by highly magnetic margins: ten subunits delineated and described on p413. The Crows Nest Granite may represent (a) roof pendants in the ?intruding Eskdale Igneous Complex, or (b) a fractionated product of the latter unit. Geochemical plot. Geochronology by Cranfield et al. (1976) and Webb and McDougall (1968) respectively.|249-233 Ma (K-Ar biotite, hornblende).||||The main body defines a zoned pluton with a core of pink, leucocratic, medium- to coarse-grained granite, through biotite-hornblende granodiorite zones, to an outer zone of hornblende-biotite granodiorite and diorite. Detailed lithologies on p413.|
31455|Esmeralda Supersuite|22533|6|Mentioned|p54,p56|Calymmian|Calymmian|Placed in Croydon Province.||||||16-JAN-07
31455|Esmeralda Supersuite|23291|3|Fully described|p33, p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Age:1558Ma (Black & McCulloch, 1990). Intrudes Etheridge and Langlo Vale Groups, Croydon Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
31455|Esmeralda Supersuite|23430|4|Described|p456-457|||S-Type chemical character. In the Croydon Province.||||||16-JAN-07
31455|Esmeralda Supersuite|23431|5|Briefly described|p530|||||||||
31455|Esmeralda Supersuite|23510|5|Briefly described|Map Legend||Mesoproterozoic|||||||
31455|Esmeralda Supersuite|24197|4|Described|p32, p76|Mesoproterozoic|Mesoproterozoic|Comprises Esmeralda, Nonda, Mooremount, Little Bird, Macartneys, Olsens, Dregger and Bimba Granites.Comagmatic with Croydon Volcanic Group. Granites, monzogranites, lesser granodiorites; felsic. Geol.Prov: Georgetown Inlier. Eg.of Hiltaba Association.||||||07-FEB-11
31455|Esmeralda Supersuite|50537|5|Briefly described|p1.1, 1.5, 3.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Age: 1550Ma. Intrudes Croydon Volcanic Group.||||||30-JUL-04
31455|Esmeralda Supersuite|63866|4|Described|p76, p78-p79, p86|Calymmian|Calymmian|Crops out in the westernmost part of the Georgetown region. Hosts tin deposits.|1558 +/- 4 Ma (TIMS, Black and McCulloch, 1990)|||Intrudes the Croydon Volcanic Group, Etheridge Group and Langlovale Group.|Coarse-grained biotite granites that have an S-type composition and are characterised by high C content.|
31455|Esmeralda Supersuite|66529|5|Briefly described|p5, p30, p92  |||Potential for a uranium field. Has strong similarities with Hiltaba Supersuite of the Gawler Craton. Appears on p93 as Esmerelda Suite.|~1560-1550 Ma (Black et al., 1998, 2005).|||Coeval with Croydon Volcanic Group.||
31455|Esmeralda Supersuite|66800|5|Briefly described|pp925-926.|Proterozoic|Proterozoic|||||Related to Croydon Volcanic Group.|High-level granites.|
31455|Esmeralda Supersuite|67323|5|Briefly described|Solid Geology Map, p22, p37, p107|Mesoproterozoic|Mesoproterozoic|See also Eastern Australia Time-Space Plot. Withnall et al. (1997). Claraville Domain. Non-magnetic. Appears as Esmeralda Suite on p22. Coeval with eruption of the Croydon Volcanic Group.|1558 +/- 4 Ma.|||Intrudes Malacura Sandstone.|Granites.|
31455|Esmeralda Supersuite|67341|6|Mentioned|vi|||Croydon Subprovince, Etheridge Province.||||||
31455|Esmeralda Supersuite|68307|5|Briefly described|p78, p85|Mesoproterozoic|Mesoproterozoic|North Australian Craton. With the Croydon Volcanic Group, shows as a very thin, nonreflective domain c.2.1 km thick. Mis-spelt as Esmerelda on p78.||||||
31455|Esmeralda Supersuite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Nonda, Mooremount and Esmeralda Granites.|||
31455|Esmeralda Supersuite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Nonda, Mooremount and Esmeralda Granites.|||
31455|Esmeralda Supersuite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Olsens, Nonda, Illewanna, Esmeralda, Dregger and Bimba Granites.||Granites, microgranite and granodiorite.|
31455|Esmeralda Supersuite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Olsens, Nonda, Illewanna, Esmeralda, Dregger and Bimba Granites.||Granites, microgranite and granodiorite.|
31455|Esmeralda Supersuite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Olsens, Nonda, Macartneys, Little Bird, Esmeralda and Chadshunt Granites.||Granites, microgranite and granodiorite.|
31455|Esmeralda Supersuite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.|||Includes Olsens, Nonda, Macartneys, Little Bird, Esmeralda and Chadshunt Granites.||Granites, microgranite and granodiorite.|
31455|Esmeralda Supersuite|68416|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Shown as younger than D2 ~ 1552 Ma.|< 1552 Ma||Includes Esmeralda Granite.|||
31455|Esmeralda Supersuite|68417|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province.|||Includes Esmeralda Granite.|||
31455|Esmeralda Supersuite|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||||||
31455|Esmeralda Supersuite|69591|4|Described|p61, p69-70, p74-75, p82-83|Mesoproterozoic|Mesoproterozoic|Georgetown Inlier. Comprises numerous granite bodies ranging in size from batholiths to stocks. Coeval with eruption of, and comagmatic with, Croydon Volcanic Group. Graphite (mostly disseminated; also pellets to 1cm) is characteristic (up to 2% by volume). The Supersuite has long been regarded as derived from partial melting of carbonaceous metasediments of the lower Etheridge Group. Other workers suggest it is I-type with assimilated country rock. Is associated with numerous gold and tin deposits; briefly discussed.|1558 +/- 4 Ma.||Esmeralda, Olsens, Macartneys, Chadshunt, Bimba, Illewanna, Dregger Granites.|Unconformably overlies and intrudes Langlovale Group; intrudes Croydon Volcanic Group and Etheridge Group.|S-type. Mostly coarse biotite granites with trace amounts of mainly secondary muscovite; some plutons contain garnet or fayalite. Contains schistose enclaves (probably restites) and xenoliths.|
31455|Esmeralda Supersuite|70207|6|Mentioned|p14|Mesoproterozoic|Mesoproterozoic|Georgetown region.||||||
31455|Esmeralda Supersuite|73163|6|Mentioned|p476|||Georgetown Inlier. Possible source of Mesoproterozoic zircons in Bandanna Formation.||||||
31455|Esmeralda Supersuite|73527|5|Briefly described|p2, p5|||Georgetown Inlier, western domain. Intruded coeval volcanic rocks.|||Esmeralda Granite, Nonda Granite, Olsen Granite, Macartney Granite||Granites, megacrystic garnet-biotite-bearing, undeformed.|
31455|Esmeralda Supersuite|73642|5|Briefly described|p3 Fig.2, p4-5, p10 Fig.8, p11-12|||Georgetown Inlier, western domain. Commonly strongly peraluminous, S-type granites except for minor components. Related to co-magmatic, rhyolitic to dacitic volcanic rocks such as the Croydon Volcanics. Abundance of enclaves and graphite increases to the west.|||Olsen Granite, Esmeralda Granite, Macartneys Granite||Granitic. Mostly non-foliated and peraluminous with abundant muscovite and biotite, and minor garnet. Commonly megacrystic and undeformed or weakly deformed.|
31455|Esmeralda Supersuite|75079|5|Briefly described|p3, 5-6, 11-12, 16-17|Mesoproterozoic|Mesoproterozoic|Western domain, Georgetown Inlier.|1550 Ma.||Esmeralda, Olsen, Macartney, Nonda Granites; Croydon Volcanic Group.|Intrudes co-magmatic Croydon Volcanic Group.|S-type. Megacrystic garnet-biotite-bearing, commonly undeformed or weakly deformed granites; includes overlying non-foliated volcanic rocks. Commonly includes dispersed sub-rounded mafic enclaves.|
25899|Ethabuka Sandstone|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Overlain by Cravens Peak beds.||||||24-JUN-04
25899|Ethabuka Sandstone|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose sandstone, mudstone.||||||19-AUG-04
25899|Ethabuka Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Late Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|12951|5|Briefly described|p143 fig 4, p145 fig 6, p149|Middle Ordovician|Early Ordovician|Toko Syncline, Georgina Basin. ||||||
25899|Ethabuka Sandstone|13995|5|Briefly described|p103|Late Ordovician|Late Ordovician|Georgina Basin. At least in part fluvial deposits.||||||
25899|Ethabuka Sandstone|22646|6|Mentioned|Fig 5 on p 105||Late Ordovician|Georgina Basin.||||||
25899|Ethabuka Sandstone|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
25899|Ethabuka Sandstone|23858|5|Briefly described|p916|||Geological Province: Georgina Basin. Max thickness: ~1150 m.||||||
25899|Ethabuka Sandstone|24442|6|Mentioned|p49|||||||||
25899|Ethabuka Sandstone|36234|6|Mentioned|Fig.1|||||||||
25899|Ethabuka Sandstone|36580|2|Defined|p469|Middle Ordovician|Middle Ordovician|||||||
25899|Ethabuka Sandstone|38832|6|Mentioned|p157|||||||||
25899|Ethabuka Sandstone|39445|5|Briefly described|Table 4|||Toko Group. See also p1.||||||18-SEP-06
25899|Ethabuka Sandstone|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25899|Ethabuka Sandstone|40136|5|Briefly described|p24|||||||||
25899|Ethabuka Sandstone|41524|6|Mentioned|Fig.3|||||||||
25899|Ethabuka Sandstone|43105|5|Briefly described|Fig.4,p9.|||||||||
25899|Ethabuka Sandstone|45155|6|Mentioned|Fig.8|||||||||
25899|Ethabuka Sandstone|46973|5|Briefly described|p52|||||||||
25899|Ethabuka Sandstone|47024|6|Mentioned|Fig.6|||||||||
25899|Ethabuka Sandstone|49027|4|Described|p20|||||||||
25899|Ethabuka Sandstone|60122|3|Fully described|p33-34, p4-5|Middle Ordovician|Middle Ordovician|Formerly Ethabuka beds, or attributed to Cravens Peak beds. Conformable over Mithaka Fm; unconformable below Cravens Peak beds and poodyea Fm; unconformably overlain by Hooray Sandstone in MOUNT WHELAN. Max. thick: 1147m in MT WHELAN. See also p10 Tb. 1.||||||18-SEP-06
25899|Ethabuka Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and quartzofeldspathic sandstone, minor siltstone and claystone.||||||
25899|Ethabuka Sandstone|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose and quartzofeldspathic sandstone, minor siltstone and claystone. Geological Province: southern Georgina Basin.||||||12-OCT-05
25899|Ethabuka Sandstone|63450|4|Described|p78 Fig. 5, p82, p84|Llanvirn|Llanvirn|Conformable over Mithaka Formation. Thickness: 1147m in AOD Ethabuka 1; <40m in outcrop. Geological province: Georgina Basin, West Toko Syncline. Contains quartzose sandstone, quartzofeldspathic sandstone, siltstone and mudstone.||||||07-FEB-11
25899|Ethabuka Sandstone|63562|6|Mentioned|p338 fig 3, p350|Late Ordovician|Late Ordovician|Of Georgina Basin. Sediment source was from uplifted areas between the Amadeus and Georgina Basins. Non-marine. Toko Syncline area.||||Correlated with Carmichael Sandstone.||06-DEC-17
25899|Ethabuka Sandstone|64068|3|Fully described|p78|Late Ordovician|Late Ordovician|||Of Toko Group.||Conformably and gradationally overlies Mithaka Formation. Is unconformably overlain by Cravens Peak beds or, where absent, Hooray Sandstone.|Sublabile to quartzose sandstone; minor siltstone and claystone interbeds; rare conglomerate.|04-APR-12
25899|Ethabuka Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
25899|Ethabuka Sandstone|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
25899|Ethabuka Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|67323|5|Briefly described|GIS attrib tbl, p83, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also Solid Geology Map. West Toko Syncline, Georgina Basin.||Toko Group||Overlies Mithaka Formation. Is overlain by Longsight Sandstone.|Quartzose to sublabile sandstone, mudstone, siltstone, clay pellet conglomerate.|
25899|Ethabuka Sandstone|67402|5|Briefly described|p25 tbl RRM3|Gisbornian|Darriwillian|Georgina Basin, West Toko Syncline. Maximum thickness of 778m. Deposited in a sub-tidal and high energy shoreline environment. See also  p213 fig GRG3, p215, p216, p217.||||Overlies the Mithaka Formation. Unconformably overlain by the Craven Peak beds.|Quartzose sandstone, quartzo-feldspathic sandtone, siltstone and mudstone.|
25899|Ethabuka Sandstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Mithaka Formation.||12-JUL-16
25899|Ethabuka Sandstone|69443|3|Fully described|p28:7, 27, 29-30|Late Ordovician|Late Ordovician|Draper (1980) after Mulready (1975). Southern Georgina Basin. Forms prominent ridges and uplands. 1147m thick in the type section in drillhole Ethabuka-1 in MOUNT WHELAN map area, Qld. In NT only c.35m of the lower part is exposed. Sedimentary structures describedl; undescribed fossil fauna listed.||Toko Group.||Conformably and gradationally overlies Mithaka Formation. Is overlain unconformably by Cravens Peak beds or Hooray Sandstone.|(Lower part): sublabile to quartzic sandstone; minor siltstone and claystone interbeds; rare conglomerate.|12-JUL-16
25899|Ethabuka Sandstone|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
25899|Ethabuka Sandstone|69591|3|Fully described|p87, p95-97|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Draper (1980). The type section is in AOD Ethabuka 1 borehole, resting on Mithaka Formation, and comprises 1147m of very fine to medium sandstone with siltstone interbeds and rare pebble layers. Up to 35m thick. (Some?) rocks of this unit, along the Toomba Range SW of Boulia, were originally mapped as Cravens Peak beds. Appears doubly mis-spelt on p87 as Ethubuka Standstone.||Toko Group.||Conformably overlies Mithaka Formation.|Fine- to medium-bedded (minor thicker beds and flaser bedding), fine-grained quartzose to sublabile sandstone overlain by friable fine sandstone with minor phosphate pellet conglomerate; some siltstone, mudstone and (in upper part) claystone beds.|
25899|Ethabuka Sandstone|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
25899|Ethabuka Sandstone|69673|5|Briefly described|p114 fig 92, p118, p119 fig 94|Ordovician|Ordovician|35m thick.||Toko Group||Overlies Mithaka Formation|Sandstone with minor siltstone and claystone interbeds with rare conglomerate.|
25899|Ethabuka Sandstone|70380|6|Mentioned|p745|Hirnantian|Katian|Southern Georgina Basin.||||||
25899|Ethabuka Sandstone|71800|6|Mentioned|p26 fig 3|Late Ordovician|Late Ordovician|Georgina Basin.||||||
77824|Etheridge Group, Upper|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
77824|Etheridge Group, Upper|64726|6|Mentioned|p83 Fig.2.|||||||||
77824|Etheridge Group, Upper|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.|||Candlow, Heliman, Townley Formations; Langdon River Mudstone.|||
77824|Etheridge Group, Upper|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Informal subdivision of Etheridge Group.||||24-FEB-14
77824|Etheridge Group, Upper|69591|5|Briefly described|p65|Paleoproterozoic|Paleoproterozoic|Encompasses the units above Robertson River Subgroup.|||Townley, Heliman, Candlow Formations and Langdon River Mudstone.|||
77824|Etheridge Group, Upper|70207|6|Mentioned|p14|Paleoproterozoic|Paleoproterozoic|Georgetown region.||||||
39236|Etonvale Formation, upper|23979|5|Briefly described|p210|||Informal - see Etonvale Formation.||||||
77825|Eulo Granite|68553|6|Mentioned|Map legend|Late Devonian|Middle Devonian|This unit and the Currawinya Granite are mapped under the same symbol, Dge.||||||
77825|Eulo Granite|68731|5|Briefly described|p166, p167 Tb 3.2|Frasnian|Givetian|S-type granite. Includes scattered phenocrysts of white K-feldspar (to ~ 5 cm), sparse inclusions of biotite schist (to ~ 10 cm); gneiss (to ~30 cm); reduced; cut by sparse, thin quartz veins; deformed; very poorly exposed. See also Eulo Ridge Granite.|385 +/- 2.5 Ma||||Pale grey to pale brownish grey, medium- to fine-grained, slightly porphyritic altered cordierite(?)-muscovite-biotite monzogranite.|03-JUL-14
77825|Eulo Granite|68823|5|Briefly described|p393|Frasnian|Eifelian|See also Eulo Ridge Granite (p378 Fig.4). Geochronology by Bultitude and Cross (2012).|385.0 +/- 2.5 Ma, SHRIMP IIe|||||
77825|Eulo Granite|68901|5|Briefly described|p5, 6, 7, p125-p127, p145|Late Devonian|Middle Devonian|Poorly exposed at Eulo Ridge, Thomson Orogen. SHRIMP age is interpreted as the age of magmatic crystallisation.|385 +/- 2.5 Ma (SHRIMP U-Pb)||||Grey, slightly porphyritic altered cordierite?-muscovite-biotite monzogranite.|16-NOV-18
77825|Eulo Granite|69952|5|Briefly described|p15-16|Late Devonian|Middle Devonian|Part of the former Eulo Ridge Granite. SHRIMP U-Pb zircon age.|385.0 +/- 2.5 Ma (Cross et al., 2012).||||Grey, slightly porphyritic, altered cordierite?-muscovite-biotite monzogranite.|
77825|Eulo Granite|70720|5|Briefly described|p2, p8|Devonian|Devonian|Eulo Ridge, southern Thomson Orogen. Small area of low magnetic intensity with minor, slight magnetic high bands.|380.0 +/- 2.5 Ma (SHRIMP U-Pb zircon).||||Grey, medium-grained equigranular biotite granite in outcrop; appears multiphase in geophysics.|
77825|Eulo Granite|70821|5|Briefly described|p9-10, p12, p13 Tb.2.1|Late Devonian|Late Devonian|The text says that an older age of ca.456 Ma has been measured for this unit; this may in fact refer to the Granite Springs Granite.|385.0 +/- 2.5 Ma (Bultitude and Cross, 2013).||||Includes monzogranite.|01-DEC-16
77825|Eulo Granite|71251|6|Mentioned|p3|||Around Eulo.||||||26-APR-18
77825|Eulo Granite|71592|5|Briefly described|Appendix A.|||Eromanga Basin.|385+/-2.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
77825|Eulo Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|385.0 +/- 2.5 Ma (Bultitude et al, 2012)||||Monzogranite.|
77825|Eulo Granite|71864|6|Mentioned|p3|||||||||
77825|Eulo Granite|71965|5|Briefly described|p897,906,913|||Geological province: Thomson Orogen. Outcropping S-type granite in the southern Thomson Orogen.|385+\-2.5 Ma||||Grey, medium-grained equigranular muscovite-biotite, cordiorite-bearing monzogranite.|
77825|Eulo Granite|71966|6|Mentioned|p989-990|Middle Devonian|Middle Devonian|Geological province: southern Thomson Orogen. Reflects a period of Middle Devonian c. 395-380 Ma magmatism.|385+\-2.5 Ma|||||
37022|Eumundi Rhyolite|23251|5|Briefly described|Table 1 p8||Late Triassic|Name used interchangeably with Eumindi Rhyolite Member. No isotopic dating; relationship to other units indicates a Late Triassic age. of SE Qld V&P Province. See Eumundi Rhyolite Member Table3 p25.||||||21-JUN-06
37022|Eumundi Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
37022|Eumundi Rhyolite|44928|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics Group. Rhyolitic ignimbrite.||||||31-MAY-06
37022|Eumundi Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland. 50-100m thick. Has petrographic similarities with Yandina Creek Rhyolite.|||||Two petrographically similar rhyolitic ignimbrite outflow sheets locally separated by clayey ash.|
37022|Eumundi Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
27975|Eureka Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
27975|Eureka Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
27975|Eureka Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V132. I-Type.||||||
27975|Eureka Rhyolite|23616|5|Briefly described|Table 3 p49||Carboniferous|Of Boonmoo Volcanic Subgroup||||||
27975|Eureka Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
27975|Eureka Rhyolite|43259|4|Described|Appendix 1,p14.||Late Carboniferous|of Boonmoo Volcanic Subgroup.||||||
27975|Eureka Rhyolite|43567|5|Briefly described|Table 2,p401|||||||||
27975|Eureka Rhyolite|43626|2|Defined|p22||Late Carboniferous|younger than 306+/-3 Ma older than 304+/- 4 Ma||||||
27975|Eureka Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27975|Eureka Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group). Age is probably Late Carboniferous?||||||07-FEB-11
33910|Eureka Supersuite|22465|5|Briefly described|p934|||||||||
33910|Eureka Supersuite|23204|6|Mentioned|p1361|||||||||
33910|Eureka Supersuite|23920|4|Described|p1068, p1087|||Geological Province: Eastern Fold Belt.||||||
33910|Eureka Supersuite|23967|5|Briefly described|p1334|||||||||
33910|Eureka Supersuite|24256|6|Mentioned|p49|||Geological Province: Mount Isa Block.||||||
33910|Eureka Supersuite|24259|6|Mentioned|p111|||Geological Province: Mount Isa Block.||||||
33910|Eureka Supersuite|65396|5|Briefly described|p55, p61, p360-361|||Mount Isa Inlier. 50-76 wt% SiO2. The product of partial melting of a variably incompatible-element-enriched gabbroic source that probably included some mantle-derived material.|||Includes Lightning Creek Granite||Diorite to syenogranite.|
33910|Eureka Supersuite|73553|6|Mentioned|p200|Calymmian|Calymmian|Williams-Naraku Igneous Province. Defined by Pollard et al., (1996) and Pollard (1998). These granites were subsequently included into the Williams Supersuite by Budd et al., (2001).|1530-1500 Ma|||||
77849|Euri Creek Granodiorite|68679|5|Briefly described|p361, p366 Fig.5.57|Permian|Permian|Northern Connors Subprovince. Early Permian. REE plot.|294.1 +/- 2.0 Ma (U-Pb SHRIMP: Cross et al. 2012).|||||
77849|Euri Creek Granodiorite|68901|5|Briefly described|p4, p94-97, p146|Sakmarian|Early Permian|New England Region. Outcrops on the northern bank of the Elliot River. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|294.1 +/- 2.0 Ma (SHRIMP U-Pb)||||Pale grey, medium-grained, slightly porphyritic biotite-hornblende granodiorite containing traces of titanite and mafic inclusions.|15-NOV-18
77849|Euri Creek Granodiorite|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, medium-grained, uneven-grained to slightly porphyritic biotite-hornblende granodiorite to hornblende-biotite tonalite; traces of titanite; deformed and partly recrystallised, with foliation in places; generally deeply weathered.|
70394|Eurimbula Granite|65452|5|Briefly described|p5, p7 Tb.2, p22, p29-30|Late Triassic|Late Triassic|Spatially, and possibly genetically, asociated with Agnes Water Volcanics. Geochemistry briefly described.||||||
70394|Eurimbula Granite|65668|5|Briefly described|p1, p2 Tb.1, p11, p13-16|Triassic|Triassic|New unit, described by recent mapping. Bundaberg area; New England Orogen. Age: 226.4 +/- 2.3 Ma (SHRIMP U-Pb zircon). Intrudes the Agnes Water Volcanics with which it has a genetic link. Pink, medium-grained, miarolitic biotite granite.||||||
70394|Eurimbula Granite|67203|5|Briefly described|p2-4|Late Triassic|Late Triassic|One of several intrusives emplaced around the time of Agnes Water Volcanics.|226.4 +/- 2.3 Ma (Cross et al., 2009).||||Granophyric, miarolitic biotite granite.|
70394|Eurimbula Granite|67874|5|Briefly described|p21, p24, p28|Late Triassic|Late Triassic|Shares aspects, such as high-level emplacement and intimate association with mafic intrusives, with Castletower Granite.|226.4 +/- 2.3 Ma (Cross et al., 2009).|||||
70394|Eurimbula Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||226.4 +/- 2.3 Ma U-Pb SHRIMP||||Pale pink, fine to medium-grained, equigranular biotite granite, commonly altered.|05-SEP-14
70394|Eurimbula Granite|68679|5|Briefly described|p428, p431 Fig.5.94, p432|Late Triassic|Late Triassic|Northern New England Orogen; Agnes Waters area. Appears as Eurimbula granite in Fig.5.94.|226.4 +/- 2.3 Ma (SHRIMP U-Pb: Cross et al., 2009)||||Pale pink, fine- to medium-grained, equigranular biotite granite; commonly altered; miarolitic.|
70394|Eurimbula Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|226+/-2.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
78924|Euroka Granodiorite|65388|2|Defined|p313-314, p301, 303, 304, p338, 340|Middle Triassic|Late Permian|New name. Previously mapped as undifferentiated Rawbelle Batholith. Of Wingfield Suite. Intruded by Late Triassic Boolgal Granophyre. Overlain by Mount Eagle Volcanics. Interpreted to be younger than Nogo beds. Fine to medium-grained, equigranular biotite-hornblende granodiorite.||||||
78924|Euroka Granodiorite|68679|5|Briefly described|p418, p420|||Rawbelle Batholith. Outcrop area ~60 km2. Geochemistry plot.||Wingfield Suite.||Is overlain by Mount Eagle Volcanics. Is intruded by Boolgal Granophyre.|Locally porphyritic hornblende-biotite granodiorite.|
37372|Eurydesma beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, fine- to medium-grained lithic arenite, dark calcareous siltstone; local limestone lenses. Thin-bedded, richly fossiliferous limestone.||||||12-DEC-07
37372|Eurydesma beds|63748|4|Described|p7 Fig. 3, p18|Early Permian|Early Permian|Unconformably overlain by Wallaby beds; faulted against older basement Silverwood Group rocks. Thickness: ~200m. Consists of conglomerate, fine-to medium-grained lithic arenite, dark calcareous siltstone and thin bedded limestone.||||||07-FEB-11
37372|Eurydesma beds|68679|5|Briefly described|p446, p452|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Exposed over 5 km2 around Rokeby homestead, 17km SE of Warwick. ~200m thick.||Wildash Group.||Is faulted against Silverwood Group. Is overlain unconformably by Wallaby beds.|Conglomerate, fine- to medium-grained lithic sandstone, calcareous siltstone and thin-bedded limestone containing early Permian marine macrofossils.|
41254|Evandale Tonalite|50597|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Foliated hornblende-biotite tonalite and granodoirite.||||||
41254|Evandale Tonalite|50598|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Medium to coarse grained, foliated hornblende-biotite tonalite and granodiorite.||||||29-JUN-04
41254|Evandale Tonalite|65388|3|Fully described|p250-251, p46, 236, 243, 248, 257, 301|Early Permian|Late Carboniferous|Intrudes Yerilla Metamorphics. Apparently intruded by Impey Granodiorite. In contact with Ah Fat Granodiorite Complex, Glisson Granodiorite, Dougherty Granite. Unconformably overlain by Evergreen Formation. Imprecise SHRIMP data suggests magmatic age ~300 Ma, 319+/-7 Ma. Part previously mapped as Kilbeggan Adamellite. Mostly pale grey, medium-grained, equigranular biotite-hornblende tonalite, but also granodiorite and rarely monzogranite. Foliated. See also p321, 432.||||||
41254|Evandale Tonalite|68008|5|Briefly described|p123|Carboniferous|Carboniferous|Possible source of detritus for Lorray Formation.|?319 +/- 7 Ma (Withnall et al., 2009).|||||
41254|Evandale Tonalite|68679|5|Briefly described|p406-407, p418-419|||Auburn Subprovince, New England Orogen. Foliated; may have undergone igneous and subsolidus deformation. Imprecise SHRIMP U-Pb zircon age determinations by Fanning et al. (2009).|~360 Ma, 325 Ma and 300 Ma.|||Intrudes Yerilla Metamorphics. May be intruded by Jack Shay Gabbro.|Mostly pale grey, medium-grained, equigranular biotite-hornblende tonalite but compositions extend to granodiorite and (rarely) monzogranite, locally quartz diorite to quartz monzodiorite. Mostly unfoliated, but some deformation in the SE.|
41254|Evandale Tonalite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Tonalite.|
27402|Eveleigh Volcanic Subgroup|23291|4|Described|p40, p95 Tb. 3.10|Permian|Carboniferous|Parent: Newcastle Range Volcanic Group. Geological Province: Georgetown Region.||||||27-MAY-15
27402|Eveleigh Volcanic Subgroup|23619|4|Described|p31 table 1||Carboniferous|Intruded by Caterpillar Microgranite. Overlying the Gilberton Formation disconformably. Of the Newcastle Range Volcanic Group.||||||
27402|Eveleigh Volcanic Subgroup|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27402|Eveleigh Volcanic Subgroup|43113|4|Described|Table 1 p19||Carboniferous|of Newcastle Range Volcanic Group.||||||
27402|Eveleigh Volcanic Subgroup|43253|5|Briefly described|map legend||Carboniferous|of Newcastle Range Volcanic Group||||||
27402|Eveleigh Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p3.||Carboniferous|||||||
27402|Eveleigh Volcanic Subgroup|43740|5|Briefly described|p12|||||||||
27402|Eveleigh Volcanic Subgroup|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group. Consists of: Shrimp Creek Rhyolite, Canyon Dacite, Mosaic Gully Rhyolite, Beril Peak Rhyolite, Pint Pot Andesite Member, Yellow Jacket Rhyolite.||||||27-MAY-15
27402|Eveleigh Volcanic Subgroup|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group. Contains the Canyon Dacite.||||||
27402|Eveleigh Volcanic Subgroup|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Newcastle Range Volcanic Group. Includes: Yellow Jacket Rhyolite, Mosaic Gully Rhyolite, Shrimp Creek Rhyolite.||||||
27402|Eveleigh Volcanic Subgroup|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Newcastle Range Volcanic Group.|Includes Canyon Dacite.|||
27402|Eveleigh Volcanic Subgroup|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Newcastle Range Volcanic Group.|Includes Yellow Jacket, Beril Peak, Mosaic Gully and Shrimp Creek Rhyolites and Canyon Dacite.|||
27402|Eveleigh Volcanic Subgroup|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.||Of the Newcastle Range Volcanic Group.|Includes Shrimp Creek Rhyolite, Mosaic Gully Rhyolite, Beril Peak Rhyolite, and Yellow Jacket Rhyolite.|||
27402|Eveleigh Volcanic Subgroup|68576|5|Briefly described|Q_11: p21|Carboniferous|Carboniferous|Forms the Eveleigh Cauldron.||Newcastle Range Volcanic Group.||||
27402|Eveleigh Volcanic Subgroup|69593|5|Briefly described|p489-490|||Kidston Subprovince, Kennedy Igneous Association.||Newcastle Range Volcanic Group.|||A-type. Broad compositional range, from dacite/granodiorite and andesite to granite and rhyolite. Intrusives are much more abundant than eruptives.|
27402|Eveleigh Volcanic Subgroup|70207|5|Briefly described|p14, p81-82|||Georgetown region. Other age determinations discussed.|316 +/- 21 Ma (Rb-Sr: Black, 1973).|Newcastle Range Volcanic Group.|||Includes welded rhyodacitic ignimbrite.|
80635|Evergreen Formation, lower|71805|6|Mentioned|p79|||Of Evans (1962) based on study of Glentulloch -1 well. Eromanga Basin. Depositional environment discussed.||||||01-SEP-20
28542|Ewan Formation|23422|5|Briefly described|p180, p205 Table 6.3|Late Carboniferous|Early Carboniferous|Of Glenrock Group.||||||
28542|Ewan Formation|23424|5|Briefly described|Fig 8.2 p328 Fig 8.4||Carboniferous|||||||
28542|Ewan Formation|23430|5|Briefly described|p506|||Of Glenrock Group. Burdekin Basin Province.||||||
28542|Ewan Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Glenrock Group.||||||23-APR-08
28542|Ewan Formation|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V64.||||||
28542|Ewan Formation|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
28542|Ewan Formation|24577|5|Briefly described|p754 Fig. 2|Late Paleozoic|Late Paleozoic|Of the Clarke River Group. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||07-NOV-08
28542|Ewan Formation|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin.||||||
28542|Ewan Formation|24613|2|Defined|p6 Fig. 3, p9 Fig. 4, p92, p105-109|Early Carboniferous|Early Carboniferous|Of Glenrock Group. Formerly Ewan beds (Wyatt et al 1970). Unconformably overlies/partly faulted against both Running River Metamorphics and Perry Creek Formation. Thickness: 720m (incomplete). Geological province: Burdekin Basin. Detailed lith. incl.||||||07-FEB-11
28542|Ewan Formation|41916|1|Redefined|p28|Early Carboniferous||||||||
28542|Ewan Formation|42295|5|Briefly described|Fig.2 P5|||||||||
28542|Ewan Formation|42407|6|Mentioned|p26, p47|||||||||
28542|Ewan Formation|42690|5|Briefly described|map legend|Carboniferous||||||||
28542|Ewan Formation|42692|5|Briefly described|map legend|Carboniferous||||||||
28542|Ewan Formation|42752|5|Briefly described|Fig.2 P46|||||||||
28542|Ewan Formation|42933|4|Described|p225|||See also Fig.73||||||
28542|Ewan Formation|43095|2|Defined|p8|Early Carboniferous||Supersedes Ewan beds.||||||23-APR-08
28542|Ewan Formation|43259|4|Described|Appendix 1,p6.||Early Carboniferous|||||||
28542|Ewan Formation|43589|6|Mentioned|p23||Early Carboniferous|Intruded by Kallanda Granite.||||||23-APR-08
28542|Ewan Formation|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Burdekin Basin.||Unit in Glenrock Group.|||Pebbly lithic arenite and conglomerate derived from Perry Creek Formation.|
28542|Ewan Formation|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Burdekin Basin.||Unit in Glenrock Group.|||Pebbly lithic arenite and conglomerate derived from Perry Creek Formation.|
28542|Ewan Formation|68731|5|Briefly described|p187|||Withnall (1990). > 750 m thick. An interval of felsic lapilli tuff is also represented. Detailed lithology discussed.||||Unconformably underlain by the Running River Metamorphics, Perry Creek Formation, and Kirk River beds.|Comprises fine lithic sandstone and conglomerate;  crystal tuff and ignimbrite interlayered with volcaniclastic conglomerate, sandstone, and mudstone; interlayered mafic lavas and poorly sorted volcaniclastics.|
28542|Ewan Formation|69593|5|Briefly described|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.||Glenrock Group.||||
80204|Excelsior Conglomerate Marker Bed|70913|4|Described|p57-58, p67 fig 9|Middle Permian|Early Permian|Gympie Province. Also referred to as the Excelsior Member on p45 fig 6, Excelsior bed p8, p44, 57, Excelsior Marker Bed p8, 11, App 1 maps,  Excelsior marker/Marker p9p/58, Excelsior conglomerate bed p49, 60. Previously referred to in GEGM reports as the Excelsior Conglomerate Marker bed. Known only from drillcore. 5-15m thick.||Base of Dawn Formation||Probably marks an unconformity between the Highbury and Dawn formations. Highbury Basalt underlies [probably unconformably].|Sandstone and conglomerate in silty hematitic matrix.|18-SEP-17
36260|Excelsior Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36260|Excelsior Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 262. I-Type.||||||
36260|Excelsior Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36260|Excelsior Granite|60425|4|Described|p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Medium- to coarse-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
29268|Exmoor Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
29268|Exmoor Formation|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
29268|Exmoor Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
29268|Exmoor Formation|23161|4|Described|p30 table4||Late Permian|||||||
29268|Exmoor Formation|23430|5|Briefly described|p515|||||||||
29268|Exmoor Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
29268|Exmoor Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Back Creek Group.  Age: >259Ma.  Geological Province: Bowen Basin.||||||
29268|Exmoor Formation|31079|6|Mentioned|Fig. 6|||||||||
29268|Exmoor Formation|31687|2|Defined|p280|Late Permian|Late Permian|See also p281-286.||||||22-OCT-08
29268|Exmoor Formation|31690|6|Mentioned|p36|||See also Fig. 2||||||
29268|Exmoor Formation|35467|6|Mentioned|p177|||||||||
29268|Exmoor Formation|36739|6|Mentioned|Fig.2|||||||||
29268|Exmoor Formation|37612|6|Mentioned|p283|||||||||
29268|Exmoor Formation|39212|4|Described|p28|||See also p11.||||||22-OCT-08
29268|Exmoor Formation|39252|6|Mentioned|Fig.13|||||||||
29268|Exmoor Formation|39261|6|Mentioned|Fig.6|||||||||
29268|Exmoor Formation|39267|5|Briefly described|p236|||||||||
29268|Exmoor Formation|39268|6|Mentioned|p269|||||||||
29268|Exmoor Formation|39445|5|Briefly described|Table 8|||||||||
29268|Exmoor Formation|40539|6|Mentioned|Fig.2|||||||||
29268|Exmoor Formation|41191|6|Mentioned|Fig.3|||||||||
29268|Exmoor Formation|41246|6|Mentioned|Map legend|Permian||||||||
29268|Exmoor Formation|41809|6|Mentioned|p63|||||||||
29268|Exmoor Formation|42249|6|Mentioned|Table 1 P22|||||||||
29268|Exmoor Formation|42250|6|Mentioned|Fig.4 P31|||||||||
29268|Exmoor Formation|42251|6|Mentioned|Fig.2 P38|||||||||
29268|Exmoor Formation|42257|5|Briefly described|Table 1 P263|||||||||
29268|Exmoor Formation|42662|6|Mentioned|p84 Fig.4|||||||||
29268|Exmoor Formation|42701|3|Fully described|p67|Late Permian||||||||
29268|Exmoor Formation|42932|6|Mentioned|Table 1|||of Jensen(1968), Malone et al (1969), Koppe (1974)||||||
29268|Exmoor Formation|44245|5|Briefly described|Map Legend||Permian|||||||
29268|Exmoor Formation|49644|5|Briefly described|Table|||||||||
29268|Exmoor Formation|50115|5|Briefly described|p55 Fig.2|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
29268|Exmoor Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: northern Bowen Basin.||||||04-FEB-08
29268|Exmoor Formation|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Quartzose to sublabile sandstone, siltstone, mudstone, rare limestone.||||||
29268|Exmoor Formation|60659|5|Briefly described|p20|Late Permian|Late Permian|Of Back Creek Gp. Sequence of very fine- to fine-grained, carbonaceous, micaceous, quartzose to sublabile sandstone and siltstone. Conformably overlies the Blenheim Fm; conformably overlain by Moranbah C.M. G.P: Bowen Basin.||||||07-FEB-11
29268|Exmoor Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
29268|Exmoor Formation|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Bowen Basin.||||Overlies Blenheim Formation.||
29268|Exmoor Formation|65388|4|Described|p190-191|Late Permian|Late Permian|This is the youngest unit (60-110m) of the Back Creek Group in the northern part of the Bowen Basin. Previously of Blenheim Subgroup and should have been reduced to member status. Most authors, including the current, have retained it as a formation . Conformably overlies Blenheim Formation. Apparently conformably overlain by Moranbah Coal Measures of Blackwater Group. May correlate with Flat Top Formation. Type section in Hillalong NS4. Generally thinly bedded, micaceous sandstone, laminated siltstone and mudstone, pyritic towards the base. Marine fossils at base and thin coal beds toward top.||||||
29268|Exmoor Formation|67402|4|Described|p21, p45, p80 tbl BWN1|Capitanian|Capitanian|Bowen Basin. Deposited in nearshore or paralic environments. See also p84, p85 tbl BWN2, p165 tbl LPB1.||||Overlies the Moonlight Sandstone. Overlain by the Fort Cooper and Moranbah Coal Measures.||
29268|Exmoor Formation|68679|5|Briefly described|p377, p381-382|Permian|Permian|Koppe (1974). Bowen Basin. 110m thick. Nearshore marine, delta complex deposits.||||Progradationally overlies Blenheim FGZ. Is overlain conformably by Moranbah Coal Measures. Lateral equivalent of lower German Creek Formation.|Quartzose to sublabile sandstone, siltstone, mudstone, minor coal; rare marine fossils.|
29268|Exmoor Formation|73036|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Quartzose to sublabile sandstone, siltstone, mudstone, rare limestone.|
29268|Exmoor Formation|73037|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Quartzose to sublabile sandstone, siltstone, mudstone, rare limestone.|
29268|Exmoor Formation|73038|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Quartzose to sublabile sandstone, siltstone, mudstone, rare limestone.|
29268|Exmoor Formation|73246|6|Mentioned|p190|Permian|Permian|Bowen Basin, northeast.||Blenheim Subgroup, Back Creek Group||Overlain by Moranbah Coal Measures (Blackwater Group).||
29268|Exmoor Formation|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Nebo Synclinorium, Bowen Basin.||||Is overlain by German Creek Coal Measures.||
36426|Expedition Creek Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p27. Type area proposed 8 km north-east of Oak Hills homestead. (8061-3547 79580). Kennedy Province.||||||
36426|Expedition Creek Granodiorite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36426|Expedition Creek Granodiorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
75751|Expedition Pass Granite|69593|5|Briefly described|p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|290 Ma.||||I-type.|
25903|Fahey Range Andesite|35812|2|Defined|p568|Triassic|Permian|Permian to Triassic||||||06-APR-10
25903|Fahey Range Andesite|36937|6|Mentioned|p229|||||||||
25903|Fahey Range Andesite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
25903|Fahey Range Andesite|38074|5|Briefly described|Table 1|||||||||
25903|Fahey Range Andesite|39079|6|Mentioned|p8|||||||||
25903|Fahey Range Andesite|39252|6|Mentioned|p27|||||||||
81490|Fair Hill Seam|70861|5|Briefly described|p38,40,42-43|Late Permian|Late Permian|Of Bowen Basin. Coal seams within the Fair Hill Formation. p40 shows Upper Fair Hill Seam and Lower Fair Hill Seam. p42, 43 shows Fair Hill and Lower Fair Hill seams. Coals are not very bright due to high mineral matter but is vitrinite-rich; accumulated peat was preserved and buried rapidly due to high sediment input and volcanic ash fall.||Unit of Fair Hill Formation.||||29-AUG-19
81490|Fair Hill Seam|73305|5|Briefly described|p551, p554 Tb.2, p555 Fig.7, p556 Fig.8|Late Permian|Late Permian|Bowen Basin. Refers to the FH1 seam (9.8 to 63.9 m thick) and underlying FH2 seam (33.4 to 112.9 m thick) collectively, where coal of the Fair Hill Formation has undergone first-order splitting. Splitting within seams becomes more common south towards the Nebo Synclinorium and includes Z-splitting. The FH1 seam splits into the Scorpio, Pegasus and Phoenix seams. The FH2 seam splits into the second-order Upper and Lower Fair Hill Seams, which in turn split into the Hercules, Canis and Lepus seams and the Fair Hill seams.||Fair Hill Formation|||Basal 5-8m thick coal ply overlain by 10-33 m of predominantly fine-grained clastic lithologies, then a 30-50 m thick sequence of thinly bedded coal, tuffs and sandstone. Includes an overlying rider coal seam (FH1 seam).|
83675|Fair Hill Seam, Lower|73305|6|Mentioned|p551, p552 Fig.4|Late Permian|Late Permian|Bowen Basin. Second-order coal seam within the Fair Hill Formation split from the FH2 seam [Fair Hill Seam]. Splits into the third-order Fair Hill seams.||Fair Hill Formation|||Coal seam.|
83676|Fair Hill Seam, Upper|73305|6|Mentioned|p551, p552 Fig.4|Late Permian|Late Permian|Bowen Basin. Second-order coal seam within the Fair Hill Formation split from the FH2 seam [Fair Hill Seam]. Splits into the Hercules, Canis and Lepus seams.||Fair Hill Formation|||Coal seam.|
83677|Fair Hill seams|73305|6|Mentioned|p551, p552 Fig.4, p556|Late Permian|Late Permian|Bowen Basin. Third-order coal seams within the Fair Hill Formation split from the Lower Fair Hill Seam.||Fair Hill Formation|||Coal seams.|12-FEB-23
82626|Fairleigh Monzogranite|71628|3|Fully described|p19: 58-60, 63-67, 70-71|||New name. Previously the Fairleigh Granite of Donchak et al. (2007). Originally part of the Herries Monzogranite of Brown et al. (2007). Named after a local homestead. Occurs 28 km WSW of Warwick as a 13 x 5 km resistant body that forms hilly country with prominent outcrops, pavements, whalebacks and large boulders. The type locality is MGA 387285 6866485 on the W side of Pikedale Road (Donchak et al., 2007). Geochemistry briefly described; assigned to Herries Suite.|253.3 +/- 2.5 Ma (SHRIMP: Li et al., 2012).|Granite Hills Complex.||Intrudes Texas beds. Abuts Clare Hills, Palgrave and Herries Monzogranites.|Pale pink to pale greyish pink or white to pale grey, moderately porphyritic hornblende-biotite monzogranite. I-type.|
78925|Fairyland Member|65388|4|Described|p160, 162, 164, 165|Artinskian|Asselian|Basal sandstone of Buffel Formation in type area. Restricted extent. Overlies Camboon Volcanics, in topographic depression. Mainly fine-grained volcaniclastic sandstone, commonly fossiliferous, and up to 45m thick. Age difficult to determine.||||||
27772|Fairymead beds|35688|3|Fully described|p353|||Insufficient information on upper boundary precludes formal definition.||||||
27772|Fairymead beds|36217|6|Mentioned|p206|||Published by Robertson 1979.||||||
27772|Fairymead beds|36581|6|Mentioned|p462|||||||||
27772|Fairymead beds|39445|5|Briefly described|Table 14|||||||||
27772|Fairymead beds|39968|6|Mentioned|p76|||||||||
27772|Fairymead beds|42895|5|Briefly described|p54|||||||||
27772|Fairymead beds|60281|5|Briefly described|p38, Fig.34 App 1|Early Eocene|Early Eocene|Fluvial sand, gravel, clay, shale and brown coal.  Overlie the Pemberton Grange Basalt.  Max. thickness: ~100m.  Geological Province: Bundaberg Trough (Maryborough Basin). ||||||
27772|Fairymead beds|61155|5|Briefly described|p20|Early Eocene|Early Eocene|Overlie Pemberton Grange and Gin Gin Basalts. Thickness: 94m. In the Bundaberg-Maryborough region. ||||||
27772|Fairymead beds|64714|4|Described|p3-4 Fig. 1, p20-23, p61 Appdx.|Early Miocene|Early Miocene|Previously included in Elliott Fm. Overlies Burrum Coal Measures; conformably overlain by Gooburrum Clay. Geol.prov: Bundaberg Trough.Unconsolidated fluviatile sand, shale, silt, gravel, + brown coal; minor clay - containing Late Miocene miospores.||||||
27772|Fairymead beds|68332|5|Briefly described|Map legend.|Miocene|Miocene|Bundaberg Trough. Subsurface only.||||Is overlain conformably by Gooburrum Clay.|Unconsolidated fluviatile sand, shale, silt, gravel and brown coal; minor clay.|
27772|Fairymead beds|68811|5|Briefly described|p162 tbl 25, p163|Tertiary|Tertiary|Hosts an aquifer system in unconsolidated alluvial sediments. See also Fairymead Beds.||||Unconformably overlies the Burrum Coal Measures. Overlain by the Gooburrum Clay.|Unconsolidated sands, gravels and clays.|14-APR-20
27772|Fairymead beds|69599|5|Briefly described|p586-587|Eocene|Eocene|Capricorn Basin. Known only in the subsurface. Fluviatile sequence. Up to 93.5m thick. A late Eocene age based on palynoflora (Foster, 1979) conflicts with age of underlying basalt and needs reassessment; discussed. RELATED UNITS (continued): Also correlated with Flinders Dolomite; Oakdale Sandstone; Lowmead and Petrie Formation; and (at least partly) with Beaudesert, Pomona, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds.||||Overlies Pemberton Grange Basalt disconformably and Burrum Coal Measures unconformably. Is overlain by Elliott Formation and Takura beds. See COMMENTS for more.|Gravel, sand, clay, brown coal and lignitic sand.|
27772|Fairymead beds|72298|5|Briefly described|p796-797|||Unconsolidated sediments contain semiconfined, unconsolidated aquifers in the Woongarra area.||||Overlies Burrum Coal Measures. Is overlain by Elliott Formation.|Unconsolidated sand, gravel and clay.|
33427|Farquharson Granite|23799|3|Fully described|p95, p11 Tb. 1|Late Triassic|Middle Triassic|Pale pinkish-grey, medium-grained,equigranular to inequigranular hornblende-biotite.  Possibly has intrusive relationship with Toondahra Granite.  Of the South-east Queensland Volcanic and Plutonic Intrusives.||||||
33427|Farquharson Granite|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
33427|Farquharson Granite|68679|5|Briefly described|p415, p428-429|Late Triassic|Late Triassic|West of the Esk Basin, northern New England Orogen.||||Intrudes Toondahra Granite.|Medium-grained, equigranular to locally porphyritic hornblende-biotite granite with prominent accessory sphene. Includes amalgamated N-trending dyke-like bodies separated by slivers of Toondahra Granite.|
31117|Fat Hen Creek Complex|22630|6|Mentioned|p 41|Ordovician|Mesoproterozoic|||||||
31117|Fat Hen Creek Complex|22844|2|Defined|p4,8,17,18,31,37-9,|Cambrian|Mesoproterozoic|Previously mapped as Ravenswood Granodiorite Complex (Paine 1979)  Intruded by Granites of the Lolworth and Reedy Springs Batholiths.||||||
31117|Fat Hen Creek Complex|23049|6|Mentioned|p22|||||||||
31117|Fat Hen Creek Complex|23283|2|Defined|p28|Ordovician|Cambrian|||||||
31117|Fat Hen Creek Complex|23422|4|Described|p174|Ordovician|Late Cambrian|Geological Province: Macrossan Province.||||||
31117|Fat Hen Creek Complex|23430|4|Described|p480|||Also see p460. Of Cape River Metamorphics, Cape River Province.||||||
31117|Fat Hen Creek Complex|23431|5|Briefly described|p537|||||||||
31117|Fat Hen Creek Complex|23499|5|Briefly described|map legend|Ordovician|Cambrian|||||||
31117|Fat Hen Creek Complex|23508|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
31117|Fat Hen Creek Complex|43480|6|Mentioned|11|||||||||
31117|Fat Hen Creek Complex|61211|5|Briefly described|p262 Fig. 1b|Late Ordovician|Late Cambrian|Deformed granites and migmatite of the Lolworth Batholith. Intrudes the Cape River Metamorphics. Max. age: 493+/-10Ma.||||||23-JAN-06
31117|Fat Hen Creek Complex|68553|6|Mentioned|Map legend|Ordovician|Cambrian|Charters Towers Province. This unit and the Shovel Creek Complex are mapped under the same symbol, -COgm.||||||
31117|Fat Hen Creek Complex|68731|5|Briefly described|p132, p136, p137, p139, p147, p216|Furongian|Furongian|Charters Towers Province. Forms a tabular sheet mappable for nearly 100 km along strike. Occurs in a discontinuous tract at the base of the Cape River Metamorphics.|~ 495 Ma, intrusive age (Fergusson et al. 2007)|||Intrudes the Gem Park Granite and the Cape River Metamorphics.|Comprises migmatitic muscovite granites, cordierite-muscovite granites and biotite granites interlayered with metasedimentary rocks and hornblende-bearing granitoids.|04-JUL-14
31117|Fat Hen Creek Complex|70744|5|Briefly described|p939|||Charters Towers Province. U-Pb zircon ages by Hutton et al. (1997).|c.495-450 Ma (estimated from Fig.7).|||||
31117|Fat Hen Creek Complex|70749|5|Briefly described|p43|Ordovician|Cambrian|Charters Towers Province. |~495-455 Ma.|||||
31117|Fat Hen Creek Complex|71592|5|Briefly described|Appendix A.|||Macrossan Igneous Province, Thomson Orogen. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|452+/-7 Ma and 441+/-10 Ma.||||Granite, gneiss, tonalite.|
31117|Fat Hen Creek Complex|71966|6|Mentioned|p989-990|Furongian|Furongian|Geological province: Charters Towers Province, Thomson Orogen. |c. 495-455 Ma|||||
31117|Fat Hen Creek Complex|73425|5|Briefly described|p14-16, 18|||Charters Towers Province, northeast Thomson Orogen. A continental arc with associated granitoid. Emplacement age is comparable to that of the Running River Metamorphics.|c.469 +/- 12 Ma (Hutton et al., 1997).|||Intrudes Cape River Metamorphics.|Orthogneiss and foliated granodiorite.|
31117|Fat Hen Creek Complex|73600|6|Mentioned|p203|Late Ordovician|Late Ordovician|Charters Towers Province.||||||
78926|Featherstone Granodiorite|65388|2|Defined|p367-368, p135 Fig. 53, p362, 383, 396|Early Permian|Late Carboniferous|Northern Connors Arch. No contacts found. Tentatively interpreted to post-date Strathdee and Carminya Granodiorites. Mount Benmore Volcanics unconformably overlie. Tentative age given. Very deeply weathered and poorly exposed. Pink or brown to dark reddish brown (weathered), medium to fine-grained, uneven-grained to slightly porphyritic muscovite-biotite monzogranite and biotite monzogranite.||||||
75752|Fence Creek Granodiorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||Tuckers Suite|||Pale pink, fine to medium-grained, uneven-grained to moderately porphyritic biotite-hornblende granodiorite; numerous inclusions to c. 30 cm (most < 10 cm) and traces of sphene, allanite; slightly granophyric and locally miarolitic.|
25906|Fenian Granite|22847|3|Fully described|p 42|Ordovician|Early Ordovician|||||||
25906|Fenian Granite|23422|5|Briefly described|p171|||See also Fenian Suite p208 Table 6.4.||||||
25906|Fenian Granite|23430|5|Briefly described|p482|||||||||
25906|Fenian Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 467. I-Type.||||||
25906|Fenian Granite|24424|5|Briefly described|p525|Ordovician|Ordovician|Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
25906|Fenian Granite|42633|5|Briefly described|Table 1 P10|||Reserved as Fenian Granodiorite.||||||
25906|Fenian Granite|42750|2|Defined|p35|Middle Ordovician|Early Ordovician|||||||
25906|Fenian Granite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Early to Middle Ordovician||||||04-JUL-14
25906|Fenian Granite|43259|4|Described|Appendix 1,p49.||Ordovician|Early - Middle Ordovician.||||||04-JUL-14
25906|Fenian Granite|43934|5|Briefly described|Map Legend||Ordovician|||||||
25906|Fenian Granite|62077|6|Mentioned|p34, p35 Fig.1, p37 Fig.2|||Ravenswood batholith.||||Intrudes Puddler Creek Formation.||
25906|Fenian Granite|62521|5|Briefly described|p11, p26|Middle Ordovician|Late Cambrian|Originally named Mount Leyshon Granite. Of the Fenian Suite (Lavery Creek Supersuite). Geological Province: Ravenswood Batholith. Medium-grained, even grained, pink to red biotite granite.||||||14-JAN-08
25906|Fenian Granite|68731|6|Mentioned|p150||||||||Comprises pink to red leucocratic biotite granite.|
38213|Fenian Suite|23422|5|Briefly described|p208 Table 6.4|||Probably Ordovician.||||||
38213|Fenian Suite|62521|5|Briefly described|p30|||Of the Lavery Supersuite.  Includes the Fenian Granite. Geological Province: Ravenswood Batholith.||||||14-JAN-08
28017|Fernhill Granite|23420|5|Briefly described|p 152 table 4.8||Early Devonian|In the Lukinville Suite of the Kintore Supersuite.||||||
28017|Fernhill Granite|23496|5|Briefly described|Table 2, p38|Devonian|Silurian|of Lukinville Suite, Kintore Supersuite.||||||
28017|Fernhill Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Lukinville Suite.||||||
28017|Fernhill Granite|43596|4|Described|p30, p26 Tb. 2, p29 Tb. 3|||Of Lukinville Suite(Kintore Supersuite). Intrudes  Daintree Gneiss and Lukinville Granodiorite(?).Moderately-strongly porphyritic biotite-muscovite granite to granodiorite+large K-feldspar and muscovite phenocrysts, scattered clots + schlieren of biotite.||||||07-APR-15
28017|Fernhill Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
38573|Fiery Suite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
38573|Fiery Suite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Fiery Creek Volcanics, Bigie Formation and Weberra Granite. Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince.||||||07-NOV-08
38573|Fiery Suite|50536|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1710Ma.||||||07-NOV-08
38573|Fiery Suite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt.||||||
30637|Fiery Supersuite|24197|4|Described|p28|||Example of the Sybella Association. Comprises Fiery Creek and Peter Creek Volcanics, and the Weberra Granite. Geological Province: western Mount Isa Inlier.||||||07-FEB-11
30637|Fiery Supersuite|50536|5|Briefly described|p7.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1710Ma. Includes: Peters Creek Volcanics, Fiery Creek Volcanics, Weberra Granite.||||||07-NOV-08
33434|Fifer Creek Metamorphics|23799|3|Fully described|p18, p15 Tb. 1|Carboniferous|Devonian|Phyllite and met-arenite with minor quartzite, gneiss and migmatite.  Intruded by  Hivesville, Wooroolin and Stuart River Granites and the Boondooma Igneous Complex.  Geological Province: Yarraman Subprovince (Wandilla Province).||||||
33434|Fifer Creek Metamorphics|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
33434|Fifer Creek Metamorphics|60371|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince. Meta-argillite, meta-arenite, meta-chert, migmatite, phyllonite; areas of shale, siltstone, arenite and chert||||||
33434|Fifer Creek Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Yarraman Subprovince. This unit, as well as Bjelke Petersen and Maronghi Creek beds, Sugarloaf and Mountefontein Metamorphics, and unnamed sedimentary units, are all mapped under the symbol, DCym.||||||
33434|Fifer Creek Metamorphics|68679|5|Briefly described|p321, p323|Carboniferous|Devonian|Cranfield et al. (2001). Northern New England Orogen. Yarraman Subprovince, Wandilla Province accretionary rocks. Forms a NW-trending, 3-4km wide and >30km long belt in the western half of the Subprovince. Represents a deeper level equivalent of the Maronghi Creek beds. Intensity of deformation, and metamorphic grade, increase with proximity to the Boondooma Igneous Complex.|||||Mudstone; siliceous, thin-bedded to laminated siltstone; variably recrystallised, quartzose to lithofeldspathic, medium- to thick-bedded sandstone; minor thin and lenticular chert beds; local brecciated, hematitic and cream chert lenses.|
33434|Fifer Creek Metamorphics|69599|6|Mentioned|p598|Carboniferous|Devonian|Gordonbrook area.||||||
29308|Fig Tree Hill Granite Complex|23500|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
29308|Fig Tree Hill Granite Complex|24485|3|Fully described|p8 Tb.1|Mesoproterozoic|Mesoproterozoic|Age: ~1550-1560Ma.  Geological Province: Etheridge Province||||||
29308|Fig Tree Hill Granite Complex|24486|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite.  Geological Province: Forsayth Sub-province (Etheridge Province).||||||
29308|Fig Tree Hill Granite Complex|43087|2|Defined|p4|Early Silurian|Mesoproterozoic|||||||
29308|Fig Tree Hill Granite Complex|44926|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29308|Fig Tree Hill Granite Complex|68405|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Etheridge Province. Includes hydrothermally altered muscovite-rich granite; minor quartz-hematite-sericite rock. Foliated granite, leucogranite comprise three of the four subdivisions of this complex.|||Informally subdivided into four units.|Younger than Einasleigh Metamorphics, McDevitt Metamorphics|Pale to medium-grey, medium-grained to pegmatitic (locally), slightly porphyritic to even-grained, (muscovite-) biotite granite and biotite-muscovite granite; enclaves of country rocks common; generally with well developed tectonic foliation.|
29308|Fig Tree Hill Granite Complex|72983|6|Mentioned|p15|Mesoproterozoic|Mesoproterozoic|||||||
23592|Finch Bay Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|Of Cooktown Supersuite.||||||01-JUN-09
23592|Finch Bay Granite|42369|3|Fully described|p42|Late Permian||Previously mapped as Findlayson Granite in 1965.||||||01-JUN-09
23592|Finch Bay Granite|42474|5|Briefly described|p27|||||||||
23592|Finch Bay Granite|43070|2|Defined|p8|Late Permian|Early Permian|Of Cooktown Supersuite.||||||01-JUN-09
23592|Finch Bay Granite|50587|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Geological Province: Kennedy Province.  Fine to medium grained, tourmaline-muscovite-biotite-granite.||||||28-JUN-04
23592|Finch Bay Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Suite (Cooktown Supersuite). S-type. Moderately porhyritic, fine- to medium-grained, cordierite (altered) -tourmaline-muscovite-biotite granite; miarolitic cavities and enclaves (including biotite-rich metasedimentary  gneiss) common.||||||07-FEB-11
23592|Finch Bay Granite|69593|5|Briefly described|p479, p481 Fig.6.5(b)|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Suite.|||S-type granitoids.|
35102|Finch Hatton Granite|23042|4|Described|p22,3,90,1 Fig 2||Carboniferous|||||||
35102|Finch Hatton Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35102|Finch Hatton Granite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Cream to light grey, fine- to medium-grained, equigranular to slightly porpyritic biotite syenogranite; minor felsic dykes. Part of the Urannah Batholith.||||||
35102|Finch Hatton Granite|65388|2|Defined|p368-369, p135, 362, 364, 365, 379, 443|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Intrudes the Palm Lookout Granodiorite. Age inferred. Fine to medium-grained, pink or cream to light grey, equigranular to seriate porphyritic biotite granite.||||||
35102|Finch Hatton Granite|68679|6|Mentioned|p366 Fig.5.57|||REE plot.||||||
72733|Fingerboard Road Granite|65452|6|Mentioned|p6 Fig.2, p22|Late Triassic|Late Triassic|Part of Agnes Water Caldera Complex. High-level emplacement.||||||
72733|Fingerboard Road Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink, fine to medium-grained, weakly porphyritic, miarolitic biotite granite; deeply weathered.|
72733|Fingerboard Road Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, fine- to medium-grained, weakly porphyritic, miarolitic biotite granite.|
36299|First Bull Run Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
36299|First Bull Run Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||White to pink, fine to medium-grained, even-grained to seriate biotite granite, with miarolitic cavities in places (commonly altered); hydrothermally altered biotite granite.|
30129|First Pocket Igneous Complex|22847|3|Fully described|p 59|Early Permian||||||||
30129|First Pocket Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Tuckers Suite.||||||
30129|First Pocket Igneous Complex|23504|5|Briefly described|Map Legend||Permian|||||||
30129|First Pocket Igneous Complex|43093|4|Described|Appendix 1|Early Permian|Early Permian|||||||
30129|First Pocket Igneous Complex|43936|5|Briefly described|Map Legend||Permian|||||||
30129|First Pocket Igneous Complex|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Tuckers Suite.||||
36355|Fish Creek Suite|23420|4|Described|p 152 table 4.8||Early Devonian|Also see p 147 table 4.6. In the Kintore Supersuite.||||||
36355|Fish Creek Suite|23496|5|Briefly described|Table 2, p41|Devonian|Silurian|of Kintore Supersuite.||||||
35395|Fitz Creek beds|61392|5|Briefly described|p164 Fig. 1|Middle Permian|Middle Permian|Of the Wildash Group.||||||07-FEB-11
35395|Fitz Creek beds|63731|5|Briefly described|Map legend|Permian|Permian|Conglomerate, volcaniclastic arenite, rhyolitic tuff. Polymictic, granule to boulder conglomerate; minor arenite and tuff. Massive, poorly sorted, dark grey rhyolitic lithi-crystal tuff, lapilli tuff and crystal tuff.||||||
35395|Fitz Creek beds|63748|4|Described|p7 Fig. 3, p20-21|Late Permian|Middle Permian|Originally mapped as Connolly Volcanics (Olgers et al 1974). Unconformably on Silverwood Group rocks, mainly Connolly Volcanics. Locally intruded by part of Herries Granite.  Max. thickness: ~1770m. Dominated by conglomerate. In the Wandsworth Province.||||||07-FEB-11
35395|Fitz Creek beds|68679|5|Briefly described|p446, p453|Permian|Permian|Olgers et al. (1974) included these rocks in the Connolly Volcanics; recognised as a separate unit by Dennis (1974) and Van Noord (1999), the latter proposing this name for two irregular areas each ~2.5 km2 about 18km S of Warwick. Silver Spur Subprovince, Woolomin Province. Estimated 314-1770m thick. Conglomerates are most common, ranging from matrix-supported to graded or inversely graded clast-supported varieties. No fossils have been recovered. Lithologically similar to nearby Rhyolite Range beds.||Wildash Group.||Unconformably overlies or is faulted against Connolly Volcanics. Is intruded by Herries Granite. May correlate with Rhyolite Range beds.|Massive thick-bedded conglomerates. Massive, poorly-sorted rhyolitic lithic-crystal tuff, lapilli tuff and crystal tuff are interbedded with minor rhyolite lava and massive, very coarse-grained volcaniclastic sandstone.|
74779|Five Mile Creek Syenogranite|61789|4|Described|p303, 310-311|Triassic|Triassic|Previously mapped as Stanthorpe Adamellite.  Age: 242.2 Ma (Shaw 1994), probably Rb-Sr. Of Stanthorpe Granite Group.||||||14-OCT-08
74779|Five Mile Creek Syenogranite|61790|6|Mentioned|p318, p319, p320|||||||||
74779|Five Mile Creek Syenogranite|71628|5|Briefly described|p11: 38; p16: 8, 11|||Sivell and Passmore (1999) after unpublished work by Passmore (1998). Previously part of Stanthorpe Monzogranite. Renamed (this study) Five Mile Creek Syenogranite Phase (of Cullendore Syenogranite).||||||
28135|Five Mile Mill Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
28135|Five Mile Mill Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
28135|Five Mile Mill Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 124. I-Type.||||||
28135|Five Mile Mill Granodiorite|23893|5|Briefly described|p15|||||||||
28135|Five Mile Mill Granodiorite|42245|2|Defined|p38|Early Devonian|Late Silurian|||||||
28135|Five Mile Mill Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
28135|Five Mile Mill Granodiorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Late Silurian to Early Devonian?. Probably related to Medowvale & Casey Spring Creek Granodiorites.||||||
28135|Five Mile Mill Granodiorite|43933|5|Briefly described|Map Legend|Devonian|Silurian|||||||
28135|Five Mile Mill Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
28135|Five Mile Mill Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Five Mile Mill gdrt.||Unit in Millchester Supersuite.||||
39102|Flaggy Quartz Monzodiorite|23799|5|Briefly described|p117|||Of the Littlemore Suite.  Geological Province: Yarrol Province.||||||
39102|Flaggy Quartz Monzodiorite|24615|5|Briefly described|CD|Permian|Permian|[Pgbf].  Grey medium- to coarse-grained foliated hypersthene-hornblende-biotite-augite quartz monzodiorite, augite-hornblende quartz monzodiorite.||||||
39102|Flaggy Quartz Monzodiorite|50317|5|Briefly described|Map Legend|Permian|Permian|Of the Bouldercombe Igneous Complex.||||||
39102|Flaggy Quartz Monzodiorite|68008|2|Defined|p131, p233, p334-337, p341-348, p350|Permian|Permian|See also p437, p484, p620. Defined in this study. Previously the southern tonalite phase of the Westwood Complex of Wood (1974). The type area is along Flaggy Creek (after which it is named) and on hillslopes around that Creek's headwaters; crops out as large flat slabs and tors and boulders. Mostly deeply weathered. Geochemistry detailed. K-Ar ages on biotite and hornblende respectively by Wood (1974) and Ford et al. (1976) recalculated to new constants. Geophysics modelling.|257 +/- 5 Ma; 258 +/- 8 Ma.|Bouldercombe Igneous Complex.||Is overlain by Precipice Sandstone. Is intruded by Umbrella Granodiorite and Bucknalla Gabbro. Intrudes Youlambie Conglomerate.|Grey to pinkish grey, medium- to coarse-grained, foliated quartz monzodiorite. Local pegmatitic patches. Foliated during emplacement. Lithology and microstructure well illustrated.|
39102|Flaggy Quartz Monzodiorite|68679|4|Described|p424, p426-427|||Yarrol Province. Arcuate, ~2km-wide unit extending ~12km along the western lobe of the Complex; surrounds the core consisting of Umbrella Creek Granodiorite. Geochemistry briefly described. Both age determinations, K-Ar biotite and K-Ar hornblende respectively, by Ford et al. (1976).|275 +/- 5 Ma and 258 +/- 9 Ma.|Bouldercombe Igneous Complex.||Is intruded by Bucknalla Gabbro and probably Umbrella Creek Granodiorite.|Foliated hypersthene-hornblende-biotite-augite-quartz monzodiorite, augite-biotite-hornblende-quartz monzodiorite. Foliation defined by lenses of more mafic material and plagioclase alignment.|
75604|Flagstaff Hill Granite|68901|5|Briefly described|p16-18, p4, p144|Aptian|Aptian|northern New England Orogen, Bowen Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.
|117.9 +/- 0.8 Ma (SHRIMP U-Pb)|||Intrudes Edgecumbe beds.|Leucocratic, pale-pink, fine-grained, slightly porphyritic, granophyric syenogranite with traces of allanite and small miarolitic cavities.|15-NOV-18
75604|Flagstaff Hill Granite|69594|5|Briefly described|p567|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.|117.9 +/- 0.8 Ma (SHRIMP: Cross et al., 2012).|||||
75604|Flagstaff Hill Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|118+/-0.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Syenogranite.|
39103|Flagstone Creek Granodiorite""|23799|5|Briefly described|p62, 63, 64|Permian|Permian|Informal name of Willey (1999). Oligoclase, quartz, orthoclase, biotite and minor hornblende.  Of the South-east Queensland Volcanic and Plutonic Intrusives.  Age: 280Ma (K/Ar - Willey, 1998).  Intrudes Sugarloaf Metamorphics.||||||11-NOV-08
39103|Flagstone Creek Granodiorite""|61781|4|Described|p269, p270, p272|Permian|Permian|Age: 283Ma (radiometic age) (Willey, 1998). Comprises Oligoclase, qtz, biotite +/- hornblende, granular to seriate, coarse grained and glomeroporphyritic mafics.||||||
36215|Flagstone Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
36215|Flagstone Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 127. Assumed to be I-Type.||||||
36215|Flagstone Granite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
41109|Flat Range Granodiorite|50301|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
41109|Flat Range Granodiorite|50597|5|Briefly described|Map Legend|Early Triassic|Late Permian|Porphyritic hornblende/biotite granodiorite, minor gabbro, monzogranite?, monzonite?.||||||
41109|Flat Range Granodiorite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Granodiorite, minor gabbro, monzogranite?, monzonite?.||||||30-JUN-04
41109|Flat Range Granodiorite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Grey, medium (locally fine) grained, porphyritic hornblende-biotite and biotite-hornblende granofiorite; minor gabbro, monzogranite?, monzonite?||||||
41109|Flat Range Granodiorite|65388|2|Defined|p314-315, 244, 248, 274, 301, 340|Early Triassic|Late Permian|Of Tandora Suite. Contacts obscured. Inferred to intrude Berri Berri Granite. In contact with Dogherty Granite. Probable age given. Mostly medium-grey, medium-grained equigranular muscovite-biotite granodiorite; some porphyritic variants.||||||
41109|Flat Range Granodiorite|68679|4|Described|p407, p419-420|Permian|Late Carboniferous|Rawbelle Batholith; Auburn Subprovince, New England Orogen. ~300 km2; mostly under Cenozoic cover: contact relationships not exposed. Geochemistry plot.|240 +/- 5 Ma (K-Ar: Webb and McDougall, 1968).|Tandora Suite.||Intrudes Berri Berri Granite.|Hornblende-biotite, biotite-hornblende granodiorite; minor gabbro.|
36227|Flat Rock Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|Of the Ootann Supersuite.||||||06-NOV-08
36227|Flat Rock Granite|23624|4|Described|p15|Permian|Carboniferous|Of the Ootann Supersuite.||||||30-JUN-15
36227|Flat Rock Granite|60425|5|Briefly described|p280-1 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. Porphyritic biotite granite.||||||07-FEB-11
36227|Flat Rock Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium-grained biotite granite.|
36227|Flat Rock Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium-grained biotite granite.|
35200|Flat Top Diorite|23042|4|Described|p107,8, Fig 2|Cretaceous|Jurassic|Possible correlation to Campwyn Volcanics.||||||
35200|Flat Top Diorite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35200|Flat Top Diorite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Hornblende diorite or gabbro; leucocratic biotite monzogranite, locally with sparse inclusions of 'diorite' and country rocks, some plutons, granophyric;diorite to quartz diorite, biotite quartz monzodiorite? to granodiorite?||||||06-NOV-08
35200|Flat Top Diorite|65388|3|Fully described|p407, p403 Fig. 135|Cretaceous|Cretaceous|Assumed to be same age as other dioritic rocks in Mackay area. Mainly dark grey, medium-grained, even-grained hornblende diorite or gabbro with biotite granite net-veining.||||||
26265|Flora Creek Trondhjemite|22847|3|Fully described|p 56|Early Devonian|Late Silurian|||||||
26265|Flora Creek Trondhjemite|23422|5|Briefly described|p213 Table 6.8|||||||||
26265|Flora Creek Trondhjemite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 468. I-Type.||||||
26265|Flora Creek Trondhjemite|42633|5|Briefly described|Table 1 P9|||Reserved.||||||
26265|Flora Creek Trondhjemite|42750|2|Defined|p44|Early Devonian|Late Silurian|||||||
26265|Flora Creek Trondhjemite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
26265|Flora Creek Trondhjemite|43259|4|Described|Appendix 1,p49.|Early Devonian|Late Silurian|||||||
26265|Flora Creek Trondhjemite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26265|Flora Creek Trondhjemite|62521|5|Briefly described|p24, p55|||Of Brittania Supersuite. Geological Province: Ravenswood Batholith. Extensively altered granitoid, characterised by presence of large composite quartz grains to about 8mm; quartz makes up 25-35% of the rock.||||||14-JAN-08
80770|Florence Creek Granite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event.||Williams Supersuite|||Pink medium-grained, equigranular biotite granite.|
80770|Florence Creek Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Pink, medium-grained, equigranular biotite granite.|
80770|Florence Creek Granite|72682|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Marimo-Staveley Domain area. Associated with Isan Orogeny (1590-1500 Ma).||Williams Supersuite||Possibly coeval with Wimberu Granite.|Pink medium-grained, equigranular biotite granite.|
80770|Florence Creek Granite|72683|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Marimo-Staveley Domain area. Associated with Isan Orogeny (1590-1500 Ma).||Williams Supersuite||Possibly coeval with Wimberu Granite.|Pink medium-grained, equigranular biotite granite.|
36106|Flynns Creek Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of O'Briens Creek Supersuite.||||||06-NOV-08
36106|Flynns Creek Granite|24485|5|Briefly described|p5, p54 Tb.8|Late Carboniferous|Late Carboniferous|||||||
36106|Flynns Creek Granite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the O'Briens Creek Supersuite.||||||
36106|Flynns Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Pale pink, fine to medium-grained, even-grained to porphyritic biotite granite; with miarolitic cavities and local small biotite-rich inclusions.|
27776|Flyspeck Supersuite|22780|5|Briefly described|map|Devonian|Late Silurian|||||||
27776|Flyspeck Supersuite|22781|4|Described|p26|Paleozoic|Paleozoic|Cape York Pennisula Batholith||||||07-NOV-08
27776|Flyspeck Supersuite|22811|6|Mentioned|p603|||of Pama Province||||||
27776|Flyspeck Supersuite|23420|4|Described|p 147 table 4.6|Early Devonian|Late Silurian|Also see p 148 table 4.7 and p 127. In the Cape York Penninsula Batholith. Age: 406+/-10Ma to 398+/- 10Ma (zircon U-Pb SHRIMP). I-type granites.||||||
27776|Flyspeck Supersuite|23430|5|Briefly described|p485|||I-Type granites. Pama Province.||||||
27776|Flyspeck Supersuite|42610|4|Described|p5, p20|||Includes all rocks assigned to Flyspeck Granodiorite in B135. The igneous equivalent of Supergroup?||||||
27776|Flyspeck Supersuite|42640|5|Briefly described|p10|||Equivalent to Flyspeck Granodiorite||||||
27776|Flyspeck Supersuite|42650|5|Briefly described|p15|||Formerly known as Flyspeck Granodiorite||||||
27776|Flyspeck Supersuite|42769|5|Briefly described|Fig.11|||||||||
27776|Flyspeck Supersuite|43596|4|Described|p24-25, p26 Tb. 2|||Major I-type component of the Siluro-Devonian Cape York Peninsula Batholith. Comprises 7 named granites:  biotite monzogranites, and hornblende-biotite monzogranites, granodiorites and tonalites.||||||07-APR-15
27776|Flyspeck Supersuite|43665|6|Mentioned|p17|||||||||
27776|Flyspeck Supersuite|43738|6|Mentioned|p5|Devonian|Silurian|||||||
27776|Flyspeck Supersuite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
27776|Flyspeck Supersuite|63154|5|Briefly described|p285 Fig. 5|Early Devonian|Early Devonian|Geological province: Coen Inlier.||||||
27776|Flyspeck Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|This unit, as well as the Blue Mountains and Kintore Supersuites, are all mapped under the same symbol, Dg.||||||
27776|Flyspeck Supersuite|69592|5|Briefly described|p282,p287-288 Figs.4.81,84,p289-290,p297|||Cape York Peninsula Batholith. Geochemistry described in some detail.|||Alberts Creek, Carleton, Gumhole, Kirkwood, Two Rail, Watch Branch, Wulpan Monzogranites; Artemis, Flyspeck, Glen Garland, Permana, Tea Tree, Yellowood Granodiorites; Peringa Tonalite.||I-type. Strongly porphyritic to even-grained biotite granite to granodiorite, hornblende-biotite granodiorite; biotite-hornblende monzogranite, granodiorite and tonalite; pyroxene-hornblende-biotite diorite.|
27776|Flyspeck Supersuite|70207|5|Briefly described|p72|Devonian|Devonian|Northern part of the Cape York Peninsula Batholith. Unit in Pama Igneous Association.|~410-395 Ma.||||I-type.|
27776|Flyspeck Supersuite|71849|5|Briefly described|p3-4, p8, p120, p122, p126, p147, p151|Devonian|Devonian|See als, p164-165, p167, p169-177, p184, p195. Comprises I-type granitoids in the south of the sheet areas studied. Geochemistry detailed. Appears as Flysheck Supersuite on p8.|||Two Rail Monzogranite, Yellowood Granodiorite.|||
27776|Flyspeck Supersuite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Kirkwood, Two Rail Monzogranites.|||
27776|Flyspeck Supersuite|72983|6|Mentioned|p91|Early Devonian|Early Devonian|||||||
27776|Flyspeck Supersuite|73179|6|Mentioned|p1152|Givetian|Pragian|Mossman Orogen, Pama Igneous Association. Geochron from Black et al. (1992).|398 +/- 10 Ma|||||26-SEP-22
27776|Flyspeck Supersuite|73387|6|Mentioned|p1, p26, p29|||I-type. Geochemically distinct from Rokeby Quartz Monzodiorite.|||Artemis Granodiorite, Glen Garland Granodiorite||Granitoids.|
83654|Focal Peak Volcanics|73581|5|Briefly described|p7||||||Albert Basalt, Kyogle Basalt||Scattered basaltic and felsic volcanic units. Includes numerous thin basal basalt lava units, interbedded with volcaniclastics.|
42166|Footwall Granodiorite|50552|5|Briefly described|p1049 Fig.3|Middle Ordovician|Early Ordovician|Overlain by Boatswain Granodiorite, separated by a fault. In Lolworth-Ravenswood Terrane.||||||24-NOV-04
35146|Footwall volcanics|23061|6|Mentioned|295|||||||||04-MAR-16
75539|Foreshores Granite|68679|5|Briefly described|p428, p432|Late Triassic|Late Triassic|Northern New England Orogen; Gladstone area.|||||Pale brown to grey, fine-grained, slightly to moderately porphyritic (augite-aegirine) biotite-arfvedsonite(?) monzogranite; locally granophyric.|
75539|Foreshores Granite|73450|4|Described|p7-8|late Triassic|late Triassic|Previously mapped as part of the Permo-Triassic Miriam Vale Granodiorite (Dear et al., 1971). Forms a small N-trending pluton SE of Tannum Sands; exposed mainly on Hummock Hill Island where it forms a broad, rounded, rise/ridge with poorly exposed, sparse, low bouldery outcrops. Thought to be late Triassic because of similar characteristics to dated late Triassic granitoids.||||Intrudes Jackass Gabbro.|Pink to red, fine-grained, leucocratic, slightly to moderately porphyritic biotite-amphibole monzogranite.|
31457|Forest Home Supersuite|22533|6|Mentioned|p54|Calymmian|Calymmian|Placed in Forsyth subprovince.||||||06-AUG-08
31457|Forest Home Supersuite|23291|3|Fully described|p33. p88 Tb. 3.7|Paleoproterozoic|Paleoproterozoic|Geological Province: Georgetown Region.||||||08-JUL-15
31457|Forest Home Supersuite|23431|5|Briefly described|p530|||||||||
31457|Forest Home Supersuite|24169|6|Mentioned|p674|||||||||
31457|Forest Home Supersuite|24197|4|Described|p19, p76|Mesoproterozoic|Mesoproterozoic|Example of the Maramungee Association. Comprises Forest Home and Talbot Creek Trondhjemites. Consists mostly of grey trondhjemites. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
31457|Forest Home Supersuite|50537|5|Briefly described|p1.1, 1.5, 2.1, 4.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Age: 1550Ma.||||||
31457|Forest Home Supersuite|63866|6|Mentioned|p75, p78|||Forsayth Subprovince, Etheridge Province.||||||
31457|Forest Home Supersuite|64722|6|Mentioned|p12|Calymmian|Calymmian|Of Georgetown-Coen region. Emplaced around 1550 Ma. Has subduction related geochemistry. Mis-spelt Forrest Home Supersuite in Fig. 2 p3-6.||||||11-APR-12
31457|Forest Home Supersuite|67341|5|Briefly described|vi, p52|||Forsayth Subprovince, Etheridge Province. Possibly contemporaneous with the Forsayth Supersuite.|||Forest Home and Talbot Creek Trondhjemites.||I-type.|
31457|Forest Home Supersuite|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Etheridge Province. This unit, the Forsayth Supersuite and the Lighthouse Supersuite are all mapped under the same symbol, -Pgf.||||||
31457|Forest Home Supersuite|69591|4|Described|p61, p82, p109-110|Paleoproterozoic|Paleoproterozoic|Champion (1991). Georgetown Inlier, Forsayth Subprovince, Etheridge Province. May include the Brandy Hot Granodiorite (discussed). May represent remnants of a potential magmatic arc, and reflect W-dipping subduction.|1563 +/- 3 Ma.||Forest Home and Talbot Creek Trondhjemites.|Intrudes Etheridge Group.|A series of small trondhjemitic I-type plutons.|
31457|Forest Home Supersuite|69592|6|Mentioned|p284|Mesoproterozoic|Mesoproterozoic||||Brandy Hot Granodiorite.|||
31457|Forest Home Supersuite|73527|6|Mentioned|p5|||Georgetown Inlier.|||||Granites.|
31457|Forest Home Supersuite|73642|5|Briefly described|p4, p10 Fig.8, p11|||Georgetown Inlier, western domain. Series of I-type plutons. Misspelt as Forrest Home Supersuite p3 Fig.2.|||Forest Home Trondhjemite, Talbot Creek trondhjemite, Brandy Hot Granite|||
31457|Forest Home Supersuite|75079|6|Mentioned|p3|||Northeast Queensland.||||||
27408|Forest Home Trondhjemite|23291|3|Fully described|p33, p88 Tb. 3.7|||Defined as Forest Home Granodiorite by Mackenzie (1980). Parent: Forest Home Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27408|Forest Home Trondhjemite|23429|5|Briefly described|p434|||||||||
27408|Forest Home Trondhjemite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 810. I-Type.||||||
27408|Forest Home Trondhjemite|24197|5|Briefly described|p19, p76|Mesoproterozoic|Mesoproterozoic|Of the Forest Home Supersuite. Age: 1550+/-50Ma (Black and Holmes, cited in Withnall et al, 1988). Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince). See also p79 Tb. 9.1.||||||07-FEB-11
27408|Forest Home Trondhjemite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27408|Forest Home Trondhjemite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27408|Forest Home Trondhjemite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
27408|Forest Home Trondhjemite|43793|5|Briefly described|p333|||U-Pb age: 1650+/-17 Ma||||||
27408|Forest Home Trondhjemite|50537|5|Briefly described|p1.1, 1.5, 4.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Age: 1550 +/- 50Ma (Rb-Sr). Geological Province: Georgetown Inlier. Intrudes: Etheridge Group.||||||
27408|Forest Home Trondhjemite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Biotite trondhjemite.||||||05-JUL-04
27408|Forest Home Trondhjemite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.|1567 +/- 10 Ma.|||||
27408|Forest Home Trondhjemite|67341|5|Briefly described|p52-56|Calymmian|Calymmian|Bain et al. (1985). Etheridge Province. Formerly Forest Home Granodiorite (Mackenzie, 1980). Comprises up to 15 small, elliptical plutons in the Black Gin Creek area. Previous age determinations mentioned. Magmatic ctystallisation age.|1564 +/- 7 Ma (SHRIMP U-Pb zircon).|Forest Home Supersuite.|||Medium- to fine-grained (rarely coarse-grained) biotite trondhjemite; local minor secondary muscovite; locally porphyritic and progressively finer-grained towards pluton margins. I-type.|
27408|Forest Home Trondhjemite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Fine- to medium-grained biotite trondhjemite.|
27408|Forest Home Trondhjemite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Fine- to medium-grained biotite trondhjemite.|
27408|Forest Home Trondhjemite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Fine- to medium-grained biotite trondhjemite.|
27408|Forest Home Trondhjemite|69591|4|Described|p82|||Comprises 15 small (up to 10km long), elliptical plutons in the Black Gin Creek area S of Forest Home homestead. Undeformed. Geochemistry briefly described. Age and genesis discussed.|1564 +/- 7 Ma (Neumann and Kositcin, 2011).|Forest Home Supersuite.||Intrudes Langdon River Mudstone and Candlow Formation (Etheridge Group).|Medium to fine biotite trondhjemite; some bodies become porphyritic and progressively finer grained towards their margins.|
27408|Forest Home Trondhjemite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|||||Trondhjemite.|
27408|Forest Home Trondhjemite|73642|5|Briefly described|p4, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier, western domain.|1564+/-14 Ma|Forest Home Supersuite||||
36298|Fork Yard Granite|23291|6|Mentioned|p40|||Geological Province: Georgetown Region.||||||08-JUL-15
36298|Fork Yard Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Creek Supersuite.||||||
29974|Forsayth Supersuite|23291|3|Fully described|p31, p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Largest known accumulation of Mesoproterozoic S-type granites. Geological Province: Forsayth Batholith||||||06-AUG-08
29974|Forsayth Supersuite|23430|5|Briefly described|p451, Table 14.1 p457|||S-Type granite.||||||
29974|Forsayth Supersuite|23431|5|Briefly described|p530|||Geological Province: Etheridge Province||||||
29974|Forsayth Supersuite|23510|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29974|Forsayth Supersuite|23616|5|Briefly described|p64-65|||S-type Granites. Dargalong Province.||||||
29974|Forsayth Supersuite|24197|4|Described|p17, p76, p77|Mesoproterozoic|Mesoproterozoic|Type example of the Forsayth Association. Includes Aurora, Delany, Forsayth, Goldsmith, Mistletoe, Ropewalk and Welfern Granites. Comprises mainly light to dark grey, biotite granite and granodiorites. Geological Province: Georgetown Inlier.||||||07-FEB-11
29974|Forsayth Supersuite|24485|5|Briefly described|p58|Mesoproterozoic|Mesoproterozoic|||||||
29974|Forsayth Supersuite|24486|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Forsayth Sub-province (Etheridge Province).||||||
29974|Forsayth Supersuite|43060|4|Described|p78|||||||||
29974|Forsayth Supersuite|43083|4|Described|p112, p114 Tb. 8|||Medium-grey, foliated, medium-grained, slightly porphyritic to even-grained biotite adamellite.||||||17-JUN-09
29974|Forsayth Supersuite|44246|6|Mentioned|Map Legend||Proterozoic|||||||
29974|Forsayth Supersuite|50537|5|Briefly described|p1.2, 1.4, 2.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Age: 1550Ma.||||||
29974|Forsayth Supersuite|63866|5|Briefly described|p75-p77, p86|||Forsayth Subprovince, Etheridge Province.|||Includes the Aura, Delaney, Forsayth, Goldsmith, Mistletoe, Ropewalk, Welfern, Mount Hogan, Fig Tree and Mywyn Granites.||Peraluminous S-type granites, dominated by grey porphyritic biotite-muscovite granite.|
29974|Forsayth Supersuite|66529|6|Mentioned|p5 ||||~1560-1550 Ma (Black et al., 1998, 2005).|||Coeval with Croydon Volcanic Group.||
29974|Forsayth Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p37|||Georgetown-Coen-Yambo Provinces. Associated with the Jana Orogeny.|1550 +/- 6 Ma.|||Intrudes Croydon Volcanic Group.|S-type.|
29974|Forsayth Supersuite|67341|5|Briefly described|vi, p46, p60, p64|Calymmian|Calymmian|Forsayth Subprovince, Etheridge Province. Main component of the Forsayth Batholith. The largest known accumulation of Mesoproterozoic granite in northern Australia. Possibly contemporaneous with the Forest Home Supersuite. |~1560-1550 Ma.||Mount Hogan, Mywyn Granites.||Peraluminous S-type granites.|
29974|Forsayth Supersuite|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Etheridge Province. This unit, the Forest Home Supersuite and the Lighthouse Supersuite are all mapped under the same symbol, -Pgf.||||||
29974|Forsayth Supersuite|69582|5|Briefly described|p76|Mesoproterozoic|Mesoproterozoic|Etheridge Province. Emplaced through a NW-SE shortening and low-pressure, high-temperature metamorphism at 1560-1550 Ma.||||Intrudes the Etheridge Group.|Mostly grey, porphyritic, biotite-muscovite granites.|
29974|Forsayth Supersuite|69591|5|Briefly described|p61, p69, p80-82, p84|Mesoproterozoic|Mesoproterozoic|Champion (1991). Georgetown Inlier, Forsayth Subprovince, Etheridge Province. Some units outside the Forsayth Batholith may belong to this Supersuite, eg Welfern, Mywyn and Mount Hogan Granites. Geochemistry described; genesis discussed.|~1560-1550 Ma.||Aurora, Delaney, Forsayth, Goldsmiths, Mount Turner, Bowler Creek, Mistletoe and Ropewalk Granites.||Mostly grey, porphyritic, biotite-muscovite granites; alkali feldspar megacrysts and muscovite are relatively common. Some rocks are strongly foliated. S-type.|
29974|Forsayth Supersuite|69592|6|Mentioned|p290|Mesoproterozoic|Mesoproterozoic|Silicic S-type intrusives; discounted as the sole or even a significant source for the Silurian I-type granitoids of the White Springs Supersuite.||||||
29974|Forsayth Supersuite|72297|6|Mentioned|p761|||High heat producing intrusives have potential for geothermal energy.||||||
29974|Forsayth Supersuite|72983|6|Mentioned|p78||||||Forsayth Granite|||
29974|Forsayth Supersuite|73163|6|Mentioned|p476|||Georgetown Inlier. Possible source of Mesoproterozoic zircons in Bandanna Formation.||||||
29974|Forsayth Supersuite|73527|5|Briefly described|p2, p5|||Georgetown Inlier, central domain. Intruded and partially melted metasedimentary rocks. [Abbreviated as Fosayth S-type granites p8?]|||Delaney Granite, Lighthouse Granite, Mistletoe Granite, Forsayth Granite, Goldsmiths Granite, Digger Creek Granite||Includes variably foliated biotite-muscovite-bearing granites.|
29974|Forsayth Supersuite|73642|5|Briefly described|p3 Fig.2, p4, p11|||Georgetown Inlier. Central domain. S-type granites, consists of about 30 individual plutons. Partially melted surrounding gneissic host rocks at mid-crustal levels.|||Forsayth Granite, Goldschmits Granite, Digger Creek Granite, Mount Hogan Granite, Hogan Granite, Mywyn Granite, Mistletoe Granite. Lighthouse Granite(?).||Variably foliated two-micas S-type granites.|
29974|Forsayth Supersuite|75079|5|Briefly described|p3-6|Mesoproterozoic|Mesoproterozoic|Central domain, Georgetown Inlier. Derived from melting of surrounding high-grade metasedimentary host rocks.|||Forsayth, Delaney, Lighthouse, Mistletoe, Goldsmiths, Digger Creek Granites.||Foliated, biotite-muscovite-bearing granites characterised by medium- to coarse-grained K-feldspar megacrysts. S-type.|
26558|Fort Cooper Coal Measures|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|22978|6|Mentioned|p148 Fig.1|||||||||
26558|Fort Cooper Coal Measures|22984|4|Described|p275|||||||||
26558|Fort Cooper Coal Measures|22986|5|Briefly described|p291|||||||||
26558|Fort Cooper Coal Measures|22988|5|Briefly described|p304|||||||||
26558|Fort Cooper Coal Measures|22989|5|Briefly described|p310|Late Permian|Late Permian|||||||
26558|Fort Cooper Coal Measures|22994|5|Briefly described|p343|||||||||
26558|Fort Cooper Coal Measures|22995|6|Mentioned|p361|||||||||
26558|Fort Cooper Coal Measures|22996|5|Briefly described|p351|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|22997|5|Briefly described|p369|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|22998|5|Briefly described|p377|||||||||
26558|Fort Cooper Coal Measures|22999|6|Mentioned|p389|||||||||
26558|Fort Cooper Coal Measures|23000|5|Briefly described|p296|||||||||
26558|Fort Cooper Coal Measures|23001|5|Briefly described|p409|||||||||
26558|Fort Cooper Coal Measures|23002|6|Mentioned|p417|||||||||
26558|Fort Cooper Coal Measures|23007|5|Briefly described|p454|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26558|Fort Cooper Coal Measures|23161|4|Described|p31 table4 fig11||Late Permian|||||||
26558|Fort Cooper Coal Measures|23430|5|Briefly described|p515-516|||Of Blackwater Group. Bowen Basin Province.||||||
26558|Fort Cooper Coal Measures|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
26558|Fort Cooper Coal Measures|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Blackwater Group.  Age: >251Ma.  Geological Province: Bowen Basin.||||||
26558|Fort Cooper Coal Measures|31079|6|Mentioned|p5|||||||||
26558|Fort Cooper Coal Measures|31401|6|Mentioned|p30|||See also P33.||||||
26558|Fort Cooper Coal Measures|31531|5|Briefly described|p14|||See also Table 1. U.Permian||||||
26558|Fort Cooper Coal Measures|31647|6|Mentioned|p358|||||||||
26558|Fort Cooper Coal Measures|31690|6|Mentioned|p35|||||||||
26558|Fort Cooper Coal Measures|32177|6|Mentioned|p146|||||||||
26558|Fort Cooper Coal Measures|35141|6|Mentioned|p159|||||||||
26558|Fort Cooper Coal Measures|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
26558|Fort Cooper Coal Measures|35873|6|Mentioned|Fig.25|||||||||
26558|Fort Cooper Coal Measures|35922|6|Mentioned|p46|||||||||
26558|Fort Cooper Coal Measures|36172|6|Mentioned|Appendix|||||||||
26558|Fort Cooper Coal Measures|36739|6|Mentioned|p24|||||||||
26558|Fort Cooper Coal Measures|37070|6|Mentioned|p73|||||||||
26558|Fort Cooper Coal Measures|37075|6|Mentioned|p110|||||||||
26558|Fort Cooper Coal Measures|37079|3|Fully described|p140|||||||||
26558|Fort Cooper Coal Measures|37080|5|Briefly described|p149|||||||||
26558|Fort Cooper Coal Measures|37612|6|Mentioned|p284|||See also Fig.3.||||||
26558|Fort Cooper Coal Measures|38518|6|Mentioned|Fig.3|||||||||
26558|Fort Cooper Coal Measures|38958|6|Mentioned|p492|||||||||
26558|Fort Cooper Coal Measures|39212|4|Described|p27|||Site near Blenheim Hst. described. See also P13||||||
26558|Fort Cooper Coal Measures|39252|6|Mentioned|Fig.13|||See also Fig.15||||||
26558|Fort Cooper Coal Measures|39261|6|Mentioned|Fig.6|||||||||
26558|Fort Cooper Coal Measures|39267|6|Mentioned|p240|||||||||
26558|Fort Cooper Coal Measures|39268|6|Mentioned|p270|||||||||
26558|Fort Cooper Coal Measures|39269|6|Mentioned|Fig.1|||||||||
26558|Fort Cooper Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9||||||
26558|Fort Cooper Coal Measures|40321|6|Mentioned|p20|||||||||
26558|Fort Cooper Coal Measures|40539|6|Mentioned|p164|||||||||
26558|Fort Cooper Coal Measures|40574|6|Mentioned|p4|||||||||
26558|Fort Cooper Coal Measures|40749|6|Mentioned|Fig.1|||||||||
26558|Fort Cooper Coal Measures|41191|6|Mentioned|p284|||||||||
26558|Fort Cooper Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
26558|Fort Cooper Coal Measures|41689|6|Mentioned|Table 1|||||||||
26558|Fort Cooper Coal Measures|41921|6|Mentioned|Fig.1|||||||||
26558|Fort Cooper Coal Measures|42249|6|Mentioned|p23|||||||||
26558|Fort Cooper Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
26558|Fort Cooper Coal Measures|42251|6|Mentioned|Fig.2 P38|||||||||
26558|Fort Cooper Coal Measures|42252|5|Briefly described|p50|||||||||
26558|Fort Cooper Coal Measures|42255|6|Mentioned|p233|||||||||
26558|Fort Cooper Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
26558|Fort Cooper Coal Measures|42257|5|Briefly described|Table 1 P263|||||||||
26558|Fort Cooper Coal Measures|42641|6|Mentioned|p119|||northern Bowen Basin||||||
26558|Fort Cooper Coal Measures|42648|5|Briefly described|p40|||||||||
26558|Fort Cooper Coal Measures|42662|6|Mentioned|p84 Fig.4|||||||||
26558|Fort Cooper Coal Measures|42701|3|Fully described|p69|||||||||
26558|Fort Cooper Coal Measures|42932|3|Fully described|p6|||see also p69||||||
26558|Fort Cooper Coal Measures|44245|5|Briefly described|Map Legend||Permian|||||||
26558|Fort Cooper Coal Measures|45095|4|Described|p10|||Type section described||||||
26558|Fort Cooper Coal Measures|50115|5|Briefly described|p55 Fig.2, p56|Late Permian|Late Permian|Fort is Ft in figure. Geological Province: Bowen Basin.||||||
26558|Fort Cooper Coal Measures|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin/Comet Ridge. Written as Fort Cooper only - Coal Measures inferred.||||||04-FEB-08
26558|Fort Cooper Coal Measures|60472|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Blackwater Group. Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.||||||27-AUG-18
26558|Fort Cooper Coal Measures|60659|5|Briefly described|p21|Late Permian|Late Permian|Of Blackwater Gp. Sequence of conglomerate, lithic sandstone, carbonaceous shale, coal and thin cherty tuff beds. Coal seams are thin to medium bedded. Conformably overlain; Rangal C.M. Geological Province: Bowen Basin.||||||07-FEB-11
26558|Fort Cooper Coal Measures|64665|5|Briefly described|p53 Fig.2.|Late Permian|Middle Permian|Bowen Basin. Heavily tuff-banded.||||Overlies Moranbah Coal Measures. Is overlain by Rangal Coal Measures.||
26558|Fort Cooper Coal Measures|65388|4|Described|p199-201|Late Permian|Late Permian|Blackwater Group, Bowen Basin. Reid (1946) but not rigidly defined. Type section given by Jensen (1975). a thickness of 400m. Conformably overlie the Moranbah Coal Measures and are overlain by the Rangal Coal Measures. Fossil wood is more common, frequently better preserved, and more opaline and siliceous than fossil wood in the Rangal Coal Measures, or Moranbah Coal Measures. Age probably Kazanian to Tatarian.||||||
26558|Fort Cooper Coal Measures|66086|5|Briefly described|Map legend|Permian|Permian|Unit in Blackwater Group. Conformably underlain by Moranbah Coal Measures. Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.||||||
26558|Fort Cooper Coal Measures|67261|6|Mentioned|p153|||Northeastern Australia.|||||Coal measures containing Glossopteris remains preserved by silicification from the breakdown of volcanic glass and unstable silicates.|
26558|Fort Cooper Coal Measures|67402|6|Mentioned|p21, p45, p80 tbl BWN1|Wuchiapingian|Wuchiapingian|Bowen Basin. See also p85, p85 tbl BWN2, p272.||Blackwater Group||Overlies the Exmoor and Blenheim Formations and the Moranbah Coal Measures. Overlain by the Rangal Coal Measures.||
26558|Fort Cooper Coal Measures|68679|5|Briefly described|p353, p377, p381-382, p384|Permian|Permian|Jensen (1975). Connors-Auburn Province. Bowen Basin. 500m thick. Alluvial plain sediments. Properties of the coal are described in some detail.||Blackwater Group.||Overlies Moranbah Coal Measures. Is overlain by Rangal Coal Measures.|Labile sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone. Numerous thick coal seams with numerous tuff bands.|
26558|Fort Cooper Coal Measures|70330|5|Briefly described|p10-16|Late Permian|Late Permian|Bowen Basin. Appears in the text as FCM after the first couple of mentions.||Blackwater Group.|Girrah, Vermont Lower, seams.|||
26558|Fort Cooper Coal Measures|70815|6|Mentioned|p3, 6, 10|||Bowen Basin. Not currently (2016) mined. Vitrinite reflectance values mapped.||||||
26558|Fort Cooper Coal Measures|70861|4|Described|p36-37,40,42-45|Late Permian|Late Permian|Of Bowen Basin. Abbreviated as FCCM in text. Average thickness: 400-450m gross. Formed during Late Permian foreland-loading in the Bowen Basin, associated with significant volcanic activity, enhanced sedimentation and change in basin configuration.||Unit of Blackwater Group.|Includes Burngrove Formation, Middle Main Seams, Kaloola Member, Black Alley Shale and Fair Hill Formation.|Overlain by Rangal Coal Measures. Underlain by Moranbah Coal Measures.|Coal seams interbedded with tuffs and carbonaceous mudstone.|29-AUG-19
26558|Fort Cooper Coal Measures|70940|4|Described|p843-844, p846, p850-851, p853|Permian|Permian|Defined by Anderson (1985). Collinsville Shelf and Nebo Synclinorium, northern Bowen Basin. Distinguished from other coal measures in the Group by its abundant tuffs, which are key marker horizons. Correlated with Fair Hill Formation, Burngrove Formation and Black Alley Shale to the SE. Abbreviated in the text to FCCM. Has a decompacted thickness of 617m, deposited in 1.34 m.y.||Blackwater Group.||Overlies Moranbah Coal Measures. Is overlain by Yarrabee Tuff. Equivalent to Kaloola Member and Gyranda Formation.|Volcanolithic, high-density coal measures.|
26558|Fort Cooper Coal Measures|71265|5|Briefly described|p589-590, p597-598, p601, p603-605|Changhsingian|Changhsingian|Eastern Galilee Basin and northern Bowen Basin. References to "Fort Cooper Coal Measures equivalent".  Sedimentary log of GSQ Muttaburra 1. Exists only where the Black Alley Shale is absent.||||Overlies Colinlea Sandstone or Moranbah Coal Measures. Is overlain by Bandanna Formation, Rangal Coal Measures or Rewan Group. Equivalent to combined Fair Hill and Burngrove Formations.||
26558|Fort Cooper Coal Measures|71276|5|Briefly described|p294 Fig.7, p295-298|Lopingian|Lopingian|Bowen Basin. The coal-bearing succession merges into this unit as the Black Alley Shale pinches out northwards. CA-IDTIMS age range by Ayaz et al. (2016).|254.03 +/- 0.26 Ma to 252.58 +/- 0.23 Ma.||||Coal with abundant tuffaceous horizons.|
26558|Fort Cooper Coal Measures|71701|5|Briefly described|p155-p159, p165-p171|Changhsingian|Changhsingian|Eastern Area and Springsure Shelf, Galilee Basin; Northern Area, Bowen Basin. [NB the author suggests that the Burngrove and Fair Hill formations are part of this unit]. Palynology of an equivalent unit discussed briefly.||||Overlies the Moranbah Coal Measures. Overlain by the Rangal Coal Measures and the Yarrabee Tuff.||
26558|Fort Cooper Coal Measures|72297|5|Briefly described|p694, p695 Fig.10.9, p750|Permian|Permian|Bowen Basin. Potential for future CSG production.||||Overlies German Creek and Macmillan Formations. Is overlain by Rangal Coal Measures. Lateral equivalent of Fair Hill and Burngrove Formations.||
26558|Fort Cooper Coal Measures|73036|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.|
26558|Fort Cooper Coal Measures|73037|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.|
26558|Fort Cooper Coal Measures|73038|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.|
26558|Fort Cooper Coal Measures|73040|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Lithic sandstone, conglomerate, mudstone, carbonaceous shale, coal, tuff, tuffaceous (cherty) mudstone.|
26558|Fort Cooper Coal Measures|73246|6|Mentioned|p190|Upper Permian|Upper Permian|Bowen Basin, northeast and northwest.||Blackwater Group||Underlain by Moranbah Coal Measures. Overlain by Rangal Coal Measures. Equivalent to Burngrove Formation and Fair Hill Formaiton.||
26558|Fort Cooper Coal Measures|73305|4|Described|p547-550, p551, p555, p560-561|Late Permian|Late Permian|Bowen Basin, northern. Abbreviated to FCCM in text. Major stratigraphic subdivisions were proposed by Anderson (1985). Upper boundary defined by the Yarrabee Tuff. Constituent coal seams merge along the Collinsville Shelf and split into the Nebo Synclinorium, Denison Trough and Taroom Trough. Hosts significant gas resources in areas of sufficient maturity. See also p553 Fig.5, p555 Fig.7, p556 Fig.8, p557 Fig.9.||Blackwater Group|Burngrove Formation, Middle Main Seams, Fair Hill Formation, Yarrabee Tuff|Overlies the Moranbah Coal Measures, underlies the Rangal Coal Measures.|Relatively thin-bedded coals of low to high density (clastic content) interbedded with clastic lithofacies and abundant tuffs, volcaniclastic and heterolithic in nature.|12-FEB-23
26558|Fort Cooper Coal Measures|73625|5|Briefly described|p5 Fig.3, p13, 20-21, p23 Fig.14D|Permian|Permian|Nebo Synclinorium, Bowen Basin.||||Overlies Moranbah Coal Measures or Black Alley Shale. Is overlain by Rangal Coal Measures.|Includes localised, plant-fossil-rich, permineralised peats associated with silica-rich ash deposits.|
76900|Foxes Creek Diorite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event.||Williams Supersuite|||Medium-coarse grained diorite to monzodiorite.|
76900|Foxes Creek Diorite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Medium- to coarse-grained diorite to monzodiorite.|
76900|Foxes Creek Diorite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Medium-coarse grained diorite to monzodiorite. Granite (mapped separately).|05-MAY-16
76900|Foxes Creek Diorite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium-coarse grained diorite to monzodiorite; includes unnamed granite.
|
72798|Foyle Volcanics|68414|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin.||||Conformably overlain by the Telemon Formation. Underlain by the Dunstable Volcanics.|Sparsely porphyritic to porphyritic basalt, andesitic to dacitic ignimbrite, and rare volcaniclastic sandstone and conglomerate and rhyolitic lava.|
72798|Foyle Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Bimurra, Silver Hills and Stones Creek Volcanics, and the Mount Wyatt and Saint Anns Formations, are all mapped under the symbol, DCD1.||||||
72798|Foyle Volcanics|68731|5|Briefly described|p173, p191|||Subdivided by Mollan et al. (1969) from the original definition of the Dunstable Formation of Hill (1957). Includes volcanics, in the Nogoa and Telemon anticlines, previously assigned to the Silver Hills Volcanics on NANDOWIE.||||Unconformably underlain by the Dunstable Volcanics.|Acid volcanics and minor sedimentary rocks.|04-JUL-14
72798|Foyle Volcanics|68900|2|Defined|p1, p4, p32-p33, p37-p38, p52-p57|Early Carboniferous|Late Devonian|Drummond Basin. Previously assigned to the Silver Hills Volcanics, however lithology has prompted reassignment to this new name. This unit is named for the Foyle homestead at GR566650 7329450 (NANDOWRIE). These rocks generally produce low hills although some flows produce prominent ridges. A type area is nominated between GR 570500 732700 and 571700 7326300. Potential age equivalent to the Silver Hills Volcanics, Vera-Nancy Volcanics and the Saint Anns Formation. Age is poorly constrained due to a lack of fossils and isotopic dating, thus ages provided are only tentative. Unconformably overlie foliated granites designated as ODg on NANDOWRIE.||||Unconformably overlies the Dunstable Volcanics. Disconformably (to unconformably) overlain by the Telemon Formation.|Basaltic volcanics including lavas and volcanogenic sediments. Some andesitic to dacitic ignimbrite and rare sedimentary rocks and rhyolite also occurs.|
72798|Foyle Volcanics|69952|6|Mentioned|p120|||Occurs in the core of the Telemon Anticline.||||||
72798|Foyle Volcanics|70857|5|Briefly described|Map Legend|Carboniferous|Devonian|||||Overlain by Telemon Formation, overlies Dunstable Volcanics|Sparsely porphyritic to porphyritic basalt, andesitic to dacitic ignimbrite, rare volcaniclastic siltstone, conglomerate and rhyolite.|
72798|Foyle Volcanics|73197|6|Mentioned|p465 Fig.4|Carboniferous|Carboniferous|Drummond Basin.|||||Volcanics.|
26562|Freitag Formation|13516|5|Briefly described|p145 fig 3, p146 fig 4, p152-154, p156|Late Permian|Late Permian|From Denison Trough, Bowen Basin. Age APP5003||||||
26562|Freitag Formation|22439|5|Briefly described|p15, Fig.2|Late Permian|Late Permian|Denison Trough, Bowen Basin.||||||
26562|Freitag Formation|22601|6|Mentioned|413|Permian|Permian|Geol Province Bowen Basin. Overlying unit Ingelara Formation||||||
26562|Freitag Formation|22872|6|Mentioned|p535, Fig.1 p536|||||||||
26562|Freitag Formation|22973|5|Briefly described|p9 Fig.2 (f)|Late Permian|Late Permian|||||||
26562|Freitag Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
26562|Freitag Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
26562|Freitag Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
26562|Freitag Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26562|Freitag Formation|24077|5|Briefly described|p410 Tb. 2|Early Permian|Early Permian|Of the Gebbie Subgroup.  Interbedded quartz sandstone, conglomeratic sandstone and mudstone, minor coal.  Max. thickness: 115m.  Geological Province: Bowen Basin.||||||
26562|Freitag Formation|29391|6|Mentioned|Table 3|||See P18.||||||
26562|Freitag Formation|29393|6|Mentioned|Table 2|||Permian.||||||
26562|Freitag Formation|29410|6|Mentioned|p274|||Geological map. Permian.||||||
26562|Freitag Formation|29412|5|Briefly described|p209|||See also Fig.2.||||||
26562|Freitag Formation|29721|6|Mentioned|p65|||||||||
26562|Freitag Formation|30449|6|Mentioned|p8|||Brachiopods||||||
26562|Freitag Formation|30450|6|Mentioned|Table 1|||Permain age. Southwest Bowen Basin||||||
26562|Freitag Formation|30508|6|Mentioned|p10|||Stratigraphic drilling. See also P91, reservoir potential||||||
26562|Freitag Formation|30826|6|Mentioned|Fig.1|||||||||
26562|Freitag Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
26562|Freitag Formation|31120|4|Described|p151|||||||||
26562|Freitag Formation|31305|6|Mentioned|p569|||||||||
26562|Freitag Formation|31690|6|Mentioned|Fig. 2|||||||||
26562|Freitag Formation|32139|6|Mentioned|p582|||See Table||||||
26562|Freitag Formation|32577|4|Described|p23|||L.Perm. See also P24,27,33,42.||||||
26562|Freitag Formation|32689|6|Mentioned|p433|||Name extended into German Cr. area||||||
26562|Freitag Formation|32840|5|Briefly described|p30|||Biostratigraphy. See also Fig.1||||||
26562|Freitag Formation|32945|6|Mentioned|p81|||See also PP82,90 & Fig.3. Permian||||||
26562|Freitag Formation|33390|4|Described|p3|||||||||
26562|Freitag Formation|33745|6|Mentioned|p204|||See also Figs 6 & 7||||||
26562|Freitag Formation|33981|5|Briefly described|p574|||||||||
26562|Freitag Formation|34132|6|Mentioned|p2|||Upper Permian||||||
26562|Freitag Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
26562|Freitag Formation|35150|6|Mentioned|p420|||||||||
26562|Freitag Formation|35284|6|Mentioned|Fig.1|||||||||
26562|Freitag Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
26562|Freitag Formation|35467|6|Mentioned|p178|||Lithology described P184||||||
26562|Freitag Formation|35845|6|Mentioned|Fig.25|||||||||
26562|Freitag Formation|35873|6|Mentioned|Fig.25|||||||||
26562|Freitag Formation|36103|4|Described|Table 1|||||||||
26562|Freitag Formation|36104|6|Mentioned|p122|||||||||
26562|Freitag Formation|36233|6|Mentioned|p152|||||||||
26562|Freitag Formation|36241|4|Described|p123|||||||||
26562|Freitag Formation|36243|6|Mentioned|Table 3A|||||||||
26562|Freitag Formation|36739|6|Mentioned|Fig.2|||||||||
26562|Freitag Formation|37070|4|Described|p72|||||||||
26562|Freitag Formation|37072|4|Described|p91|||||||||
26562|Freitag Formation|37450|5|Briefly described|p374|||||||||
26562|Freitag Formation|37612|6|Mentioned|p283|||||||||
26562|Freitag Formation|37705|6|Mentioned|Fig.2|||||||||
26562|Freitag Formation|37724|6|Mentioned|Table 1|||||||||
26562|Freitag Formation|37726|3|Fully described|p146|||||||||
26562|Freitag Formation|38092|6|Mentioned|p284|||||||||
26562|Freitag Formation|38204|6|Mentioned|p79|||||||||
26562|Freitag Formation|38312|4|Described|p461|||||||||
26562|Freitag Formation|38955|4|Described|p314|||||||||
26562|Freitag Formation|39212|5|Briefly described|p11|||P24 gas reservoir. Excursion sites. See also P33 & 35||||||
26562|Freitag Formation|39219|6|Mentioned|p46|||Microflora||||||
26562|Freitag Formation|39252|6|Mentioned|Fig.13|||||||||
26562|Freitag Formation|39261|6|Mentioned|Fig.6|||||||||
26562|Freitag Formation|39263|6|Mentioned|Fig.2|||||||||
26562|Freitag Formation|39264|6|Mentioned|Fig. 13|||||||||
26562|Freitag Formation|39267|6|Mentioned|p237|||||||||
26562|Freitag Formation|39268|6|Mentioned|p269|||||||||
26562|Freitag Formation|39272|6|Mentioned|p295|||||||||
26562|Freitag Formation|39273|4|Described|p309|||||||||
26562|Freitag Formation|39275|6|Mentioned|p332|||||||||
26562|Freitag Formation|39412|6|Mentioned|p13|||||||||
26562|Freitag Formation|39423|6|Mentioned|p47|||||||||
26562|Freitag Formation|39494|6|Mentioned|Fig.5|||||||||
26562|Freitag Formation|39611|6|Mentioned|Fig.2|||||||||
26562|Freitag Formation|39815|6|Mentioned|Fig.10|||||||||
26562|Freitag Formation|39943|6|Mentioned|Table 5A|||||||||
26562|Freitag Formation|40030|6|Mentioned|Fig.5|||||||||
26562|Freitag Formation|40250|6|Mentioned|Table 6|||||||||
26562|Freitag Formation|40539|6|Mentioned|Fig.2|||||||||
26562|Freitag Formation|40544|6|Mentioned|Fig.6|||||||||
26562|Freitag Formation|40623|5|Briefly described|p110|||||||||
26562|Freitag Formation|40675|6|Mentioned|Table 5A|||||||||
26562|Freitag Formation|41173|6|Mentioned|Table 2|||||||||
26562|Freitag Formation|41246|6|Mentioned|Map legend|Permian||||||||
26562|Freitag Formation|41247|6|Mentioned|Fig.7|||||||||
26562|Freitag Formation|41275|6|Mentioned|p30|||||||||
26562|Freitag Formation|41330|6|Mentioned|Table 1|||||||||
26562|Freitag Formation|41605|6|Mentioned|Fig. 2|||||||||
26562|Freitag Formation|41666|6|Mentioned|p27|||||||||
26562|Freitag Formation|41737|6|Mentioned|p351|||||||||
26562|Freitag Formation|42187|6|Mentioned|p318|||||||||
26562|Freitag Formation|42249|6|Mentioned|Fig.3 P24|||||||||
26562|Freitag Formation|42250|6|Mentioned|p33|||||||||
26562|Freitag Formation|42253|5|Briefly described|Fig.2 P217|||||||||
26562|Freitag Formation|42254|6|Mentioned|p221|||||||||
26562|Freitag Formation|42437|6|Mentioned|Fig.3 P822|||||||||
26562|Freitag Formation|42578|5|Briefly described|Table 1 P124-125|||||||||
26562|Freitag Formation|42621|6|Mentioned|p274|||||||||
26562|Freitag Formation|42641|6|Mentioned|Fig.3 P110|||||||||
26562|Freitag Formation|42648|6|Mentioned|Fig.6 P41|||||||||
26562|Freitag Formation|42856|5|Briefly described|Fig.9 P642|||||||||
26562|Freitag Formation|42865|5|Briefly described|p18|||||||||
26562|Freitag Formation|42911|6|Mentioned|p8|||||||||
26562|Freitag Formation|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
26562|Freitag Formation|43017|5|Briefly described|Fig.3,p375|||||||||
26562|Freitag Formation|43050|5|Briefly described|p4|||||||||
26562|Freitag Formation|43185|6|Mentioned|6-10||Late Permian|||||||
26562|Freitag Formation|43213|5|Briefly described|p152|||Power (1966), who regarded this as a separate unit. Mollan et al., (1969), included it as the upper of three informal members of the Aldebaran Sandstone.||||Overlies Aldebaran Sandstone conformably and locally disconformably.|Thinly interbedded sandstone, siltstone and mudstone with minor coal seams.|
26562|Freitag Formation|43580|6|Mentioned|Fig.1,p360|||||||||
26562|Freitag Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
26562|Freitag Formation|43737|6|Mentioned|p5||Sakmarian|||||||
26562|Freitag Formation|44091|14|Not recorded|p45,Tb.3,p47|||Part of Middle Bowen Group in Springsure area.||||||
26562|Freitag Formation|44172|2|Defined|p1323,1327-8,1330-4,||Artinskian|p1340,1342-4 Fig.2,Tb.1. Springsure area.||||||
26562|Freitag Formation|44173|2|Defined|p109-113||Early Permian|Unconformably overlies Aldebaran Sandstone. Overlain by Ingelara Formation.||||||
26562|Freitag Formation|44424|14|Not recorded|p293-301|||Upper member of Aldebaran Sandstone||||||
26562|Freitag Formation|44618|14|Not recorded|p517||Permian|||||||
26562|Freitag Formation|46849|6|Mentioned|p192|||||||||
26562|Freitag Formation|46989|5|Briefly described|Table 1|||||||||
26562|Freitag Formation|48900|6|Mentioned|Table 3|||||||||
26562|Freitag Formation|48995|6|Mentioned|Fig.3|||||||||
26562|Freitag Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin/Comet Ridge.||||||
26562|Freitag Formation|60286|4|Described|p274|Late Permian|Late Permian|Overlies Upper Aldebaran Sandstone. Overlain by Ingelara Formation. Offshore and shelf to coastal facies. Geological Province: Bowen Basin.||||||09-FEB-05
26562|Freitag Formation|60330|5|Briefly described|p261 Fig.2|Kazanian|Kazanian|||||||
26562|Freitag Formation|61377|6|Mentioned|p156 Tb. SU2|Early Permian|Early Permian|A reservoir unit in Queensland.||||||07-FEB-11
26562|Freitag Formation|61609|6|Mentioned|p240|Permian|Permian|Geological Province: Denison Trough.||||||07-FEB-11
26562|Freitag Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
26562|Freitag Formation|62357|5|Briefly described|p524 Fig. 7|Late Permian|Middle Permian|Geological Province: Bowen Basin.||||||
26562|Freitag Formation|63713|5|Briefly described|p1507 Fig.2, p1508, p1522-1523, p1526|Roadian|Kungurian|See also p1528-1533, p1535. Denison Trough, Bowen Basin. Graphic log. Well-log correlation. A successful hydrocarbon exploration target.||||Overlies Aldebaran Sandstone. Is overlain by Ingelara Formation.|A lower coarsening-upward interval, overlain by a complex series of heterolithic mudrock and sandstone intervals.|
26562|Freitag Formation|63832|5|Briefly described|p131 fig 2, p137|Wordian||West Bowen Basin. Appears in Fig.2 as Cath./Freit./Ing. Contains distal glaciomarine facies (outsized basement clasts in mudrock, glendonites) recording the final (P4) Paleozoic glaciation. Resembles Pebbley Beach Formation.|||||A relatively thin unit composed of a series of short, condensed and top-truncated, unconformity-bounded sequences with limited sediment supply.|13-DEC-17
26562|Freitag Formation|64631|6|Mentioned|p48 Fig.4, p49.|Wordian|Wordian|Bowen Basin. Contains distal glaciomarine facies, eg glendonites and outsized basement clasts in mudrocks. See also p44 where shown with Catherine Sst, Ingelara Fm. Some biostratigraphic age control indicated.||||||
26562|Freitag Formation|64857|6|Mentioned|p119, p113 Fig.3|Late Permian|Late Permian|Denison Trough, Bowen Basin.||||||
26562|Freitag Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Denison Trough, Bowen Basin. Underlies Ingelara Formation and overlies Upper Aldebaran Sandstone.||||||14-SEP-09
26562|Freitag Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Denison Trough. Overlies upper Aldebaran Sandstone, underlies Ingelara Formation.||||||
26562|Freitag Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
26562|Freitag Formation|65115|5|Briefly described|p413, 415, Fig 2 p403|Kazanian|Ufimian|Overlies the upper Aldebaran Formation, underlies the Ingelara Formation in the Denison Trough, Bowen Basin. Part of Supersequence D.||||||
26562|Freitag Formation|65116|5|Briefly described|p447, Fig 2 p436|Late Permian|Late Permian|Underlies the Ingelara Formation, overlies the upper Aldebaran Sandstone in the Denison Trough, Bowen Basin. Sequence boundary at base.||||||
26562|Freitag Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|?Underlies the Ingelara Formation, overlies the upper Aldebaran Sandstone Denison Trough, Bowen Basin.||||||06-MAR-12
26562|Freitag Formation|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p7, p8|||Denison Trough, Bowen Basin.||||||
26562|Freitag Formation|67402|6|Mentioned|p21, p64, p65, p68-p70|Capitanian|Capitanian|Bowen Basin. Approximately 90m thick. Deposited in either a deltaic or nearshore marine environment. Alternatively a reservoir and a seal for the underlying Aldebaran Sandstone. See also  p72, p73, p76-p79, p165 tbl LPB1, p302. ||||Overlies the Aldebaran Sandstone, Upper. Overlain by the Ingelara Formation.|Interbedded sandstone, siltstone and sandy mudstone.|
26562|Freitag Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Ingelara Formation. Underlain by, and laterally equivalent to Aldebaran Siltstone.||
26562|Freitag Formation|68576|5|Briefly described|Q_4: p3, p9, p19|Lopingian|Lopingian|Bowen Basin. Represents a marine transgression.||||Overlies Aldebaran Sandstone. Is overlain by Ingelara Formation.|Interbedded sandstone (in part pebbly), siltstone and sandy mudstone; wavy, irregular bedding and bioturbation are common.|
26562|Freitag Formation|68679|5|Briefly described|p378, p380-381, p384|Permian|Permian|Power (1967). Denison Trough, Bowen Basin. 120m thick. Prograding coastal plain sediments. Produces gas and minor condensate.||||Overlies Aldebaran Sandstone. Is overlain by Maria and Ingelara Formations.|Interbedded sandstone, siltstone, mudstone; coal seams to the north.|
26562|Freitag Formation|68731|6|Mentioned|p201 Fig 3.110|Late Permian|Late Permian|Bowen Basin.||||||
26562|Freitag Formation|71265|5|Briefly described|p589-590, p595, p602, p606|Wuchiapingian|Wuchiapingian|Bowen and eastern Galilee Basins. Sedimentary log of GSQ Tambo 1-1A. Terrestrial deposits.||||Overlies Aldebaran Sandstone. Is overlain by Ingelara Formation.|Fluvial sediments capped by a 3.5m-thick coal seam.|
26562|Freitag Formation|71276|5|Briefly described|p294, p295 Fig.8, p296-297|Permian|Permian|Denison Trough, Bowen Basin.||||Overlies Aldebaran Sandstone. Is overlain by Ingelara Formation (= Maria and Blenheim Formations). Probable lateral equivalent of (part of) the Colinlea Sandstone.|Interbedded sandstone and siltstone.|
26562|Freitag Formation|71701|5|Briefly described|p155-p156, p168|Changhsingian|Wuchiapingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Aldebaran Sandstone, upper. Overlain by the Ingelara Formation. Equivalent to the Rodney Creek Sandstone.||
26562|Freitag Formation|72088|5|Briefly described|p8, p20, p38, p91|Wuchiapingian|Wuchiapingian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Aldebaran Sandstone. Overlain by the Ingelara Formation.||
26562|Freitag Formation|72297|5|Briefly described|p695|||Bowen Basin.|||||Contains coal in thin seams and below coking rank.|
26562|Freitag Formation|73304|6|Mentioned|p77|||Bowen Basin.||||||
26562|Freitag Formation|73472|6|Mentioned|p115|Wuchiapingian|Wuchiapingian|Galilee Basin.||||Underlain by Aldebaran Sandstone. Overlain by Ingelara Formation. Equivalent to Colinlea Sandstone.||
26562|Freitag Formation|73625|6|Mentioned|p2-3|Permian|Permian|Bowen Basin.||||Overlies upper Aldebaran Sandstone. Is overlain by Ingelara Formation.||
77811|Frenchy Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Coarsely porphyritic biotite granite.|
69500|Frog Hollow Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium- to fine-grained biotite granite, commonly altered.|
69500|Frog Hollow Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium- to fine-grained biotite granite, commonly altered.|
77802|Fulford Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Fine to medium-grained, porphyritic (muscovite-) biotite granite.|
27288|Furry Hoop Member|23032|5|Briefly described|p36|Visean|Visean|Within "lower" Lyall Formation.||||||
27288|Furry Hoop Member|23424|5|Briefly described|Table 8.1 Fig 8.4 p338.||Visean|In the lower part of Lyall Formation. Of Lyall Formation/Clarke River Group. Geological Province Clarke River Basin.||||||
27288|Furry Hoop Member|23430|5|Briefly described|p508|||Of Lyall Formation. Clarke River Basin Province.||||||
27288|Furry Hoop Member|40943|2|Defined|p56|late Visean|late Visean|Previously part of Clarke River Formation||||||
27288|Furry Hoop Member|41260|5|Briefly described|p23|||||||||
27288|Furry Hoop Member|41776|5|Briefly described|p527|||||||||
27288|Furry Hoop Member|41823|5|Briefly described|p162|||||||||
27288|Furry Hoop Member|41824|6|Mentioned|p201|||||||||
27288|Furry Hoop Member|42692|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
27288|Furry Hoop Member|42933|4|Described|p212|||of Lyall Formation||||||
27288|Furry Hoop Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Lyall Formation.||||||
27288|Furry Hoop Member|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Lyall Formation.|||Red, purple and green, calcareous siltstone and mudstone; minor volcanilithic sandstone and conglomerate.|
27288|Furry Hoop Member|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Lyall Formation.|||Red, purple and green, calcareous siltstone and mudstone; minor volcanilithic sandstone and conglomerate.|
39071|Gaeta Diorite|64556|5|Briefly described|p36-40, p56|Late Permian|Late Permian|Age for magmatic emplacement: 262.6+/-2.5Ma. Age analysis details included. Sample analysed is massive orthopyroxene (+/-clinopyroxene) + plagioclase )+/-biotite) diorite; locally coarse- and fine- grained varieties are present.||||||07-FEB-11
39071|Gaeta Diorite|65452|5|Briefly described|p7 Tb.2|Guadalupian|Guadalupian|SHRIMP U-Pb zircon magmatic crystallisation age.|262.6 +/- 2.5 Ma (Carson et al. 2006).||||Orthopyroxene (+/- clinopyroxene?), hornblende, plagioclase (+/- biotite) diorite.|
39071|Gaeta Diorite|68421|5|Briefly described|Map Legend|Capitanian|Capitanian|The 2 facies are mapped separately. U-Pb dating by Carson et al, 2006 GSQ Rec2006/1|262.6 +/- 2.5 Ma (zircon U-Pb age).||||Dark grey to black, fine to medium-grained, equigranular, hornblende diorite; medium to coarse-grained, equigranular hornblende gabbro; pegmatite, in places containing tourmaline.|05-SEP-14
39071|Gaeta Diorite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|262.6 +/- 2.5 Ma (SHRIMP: Carson et al., 2006).||||Hornblende diorite, hornblende gabbro.|
39071|Gaeta Diorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|269+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite, diorite.|
39071|Gaeta Diorite|73450|6|Mentioned|p21-22|||Interpreted to pre-date Molangul Granite and Borilla Granite.||||||
83549|Galah Tuff Bed|73472|2|Defined|p113, p118, p123, p126-129, p131, App.2|Olenekian|Wuchiapingian|Galilee Basin. Occurs ca 4 m below the top of the Betts Creek beds. Named for the parish of Galah. Type area is within Porcupine Gorge. Maximum thickness of 1.5 m; average thickness of 0.5 m. A U-Pb LA-ICP-MS zircon age of 251.9 +/- 3 Ma was reported herein. May be genetically related to the Gibraltar Ignimbrite [based on matching ages]. [See supplementary materials for unit definition].|251.9 +/- 3 Ma U-Pb LA-ICP-MS|Betts Creek beds||Equivalent to Yarrabee Tuff.|White, porphyritic, and typically internally massive ash-fall tuff.|
27411|Gallangowan Granodiorite|22845|6|Mentioned|p46,59,61,8,9,71,7,8||Late Carboniferous|||||||
27411|Gallangowan Granodiorite|22846|2|Defined|p6-12,18,20,41,75|Late Triassic|Namurian|||||||
27411|Gallangowan Granodiorite|23251|6|Mentioned|p29||Late Carboniferous|Of Crouch & others (1995) Synkinematic S-type granitoid.||||||
27411|Gallangowan Granodiorite|23608|4|Described|p50 Fig 1||Carboniferous|319 Ma. Transitional S- to I-type granite. Of Wratten Igneous Suite. North D'Aguilar Block.||||||
27411|Gallangowan Granodiorite|23609|5|Briefly described|p7, 9|||North D'Aguilar Block.||||||
27411|Gallangowan Granodiorite|23799|5|Briefly described|p23, p123|Early Permian|Late Carboniferous|Geological Province: North D'Aguilar Province.||||||
27411|Gallangowan Granodiorite|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27411|Gallangowan Granodiorite|35101|3|Fully described|p66|||||||||
27411|Gallangowan Granodiorite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
27411|Gallangowan Granodiorite|36528|6|Mentioned|p174|||||||||
27411|Gallangowan Granodiorite|37252|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27411|Gallangowan Granodiorite|37376|6|Mentioned|Table 1|||||||||
27411|Gallangowan Granodiorite|39445|5|Briefly described|Table 12|||||||||
27411|Gallangowan Granodiorite|41917|6|Mentioned|p522|||||||||
27411|Gallangowan Granodiorite|43092|6|Mentioned|p24|||||||||
27411|Gallangowan Granodiorite|43588|6|Mentioned|p30||Late Carboniferous|||||||
27411|Gallangowan Granodiorite|44923|5|Briefly described|Map Legend||Carboniferous|||||||
27411|Gallangowan Granodiorite|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27411|Gallangowan Granodiorite|60077|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Coarse-grained, grey, porphyritic granodiorite.||||||19-JUL-04
27411|Gallangowan Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Capsize Creek Complex; the Coppermine Creek, Claddagh, Karandah and Yabba Creek Granodiorites, are all mapped under the same symbol, Cgd.||||||
27411|Gallangowan Granodiorite|68679|4|Described|p320, p323, p325-326, p331, p386-387|Late Carboniferous|Late Carboniferous|See also p403-405, p470. Kilkivan-Manumbar area, North D'Aguilar Subprovince. Syntectonic granitoids. A source of detritus in overlying Marumba beds and (probably) Kandanga Creek Megabreccia.|319.1 +/- 10 Ma (K-Ar biotite: McNaughton, 1973).|Wratten Igneous Suite.||Thrust over Amamoor beds; unconformably underlies Marumba beds.|Highly deformed, foliated, medium- to coarse-grained, biotite-rich, garnet-bearing granodiorite.|
38881|Galloway Plains Igneous Complex|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
38881|Galloway Plains Igneous Complex|50197|5|Briefly described|Map Legend|Triassic|Permian|Includes: Voewood Granite, Bocoolima Granodiorite, Redshirt Granite, Wyalla Granite, Rocky Point Granodiorite, Dumgree Tonalite, Sawnee Gabbro.||||||
38881|Galloway Plains Igneous Complex|68008|4|Described|p40, p330, p361, p372-390, p422-423|||See also p528, p624, p626-630. Previously the Galloway Plains Tonalite of Dear et al. (1971) for a small batholith 45km NE of Biloela. They described it as consisting solely of grey tonalite, apart from a small outlier of Muncon Volcanics. Airborne geophysics and field mapping have subsequently led to seven named and one unnamed unit, within the Galloway Plains Igneous Complex. Geophysics modelling. Appears as Galloway Plains Intrusive Complex on p627.|||Bocoolima, Rocky Point Granodiorites; Sawnee Gabbro; Dumgree Tonalite; Wyalla, Redshirt, Voewood Granites.|Intrudes Raspberry Creek Formation.||
38881|Galloway Plains Igneous Complex|68679|5|Briefly described|p410, p424-425|||Yarrol Province. A multiphase batholith. Includes an unassigned small body on the western extremity of the Complex. Appears as Galway Plains Igneous Complex on p410.|||Bocoolima Granodiorite, Dumgree Tonalite, Sawnee Gabbro, Redshirt, Voewood and Wyalla Granites.|Intrudes Youlambie Conglomerate and Inverness Volcanics.|Unassigned: biotite-hornblende quartz diorite and augite-hypersthene-hornblende-quartz gabbro. See also individual CONSTITUENTS.|
36286|Galloway Volcanic Group|23291|3|Fully described|p41, p93 Tb. 3.9|Early Permian|Late Carboniferous|Formerly "Galloway Volcanics". Geological Province: Georgetown Region.||||||08-JUL-15
36286|Galloway Volcanic Group|23510|5|Briefly described|Map Legend||Early Permian|||||||
36286|Galloway Volcanic Group|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork, Mitchell River and Nychum Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
36286|Galloway Volcanic Group|69593|5|Briefly described|p484-485, p510|Late Carboniferous|Late Carboniferous|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Campbell Mountain cauldron. Sm-Nd isotope data tabulated.|290 +/- 3 Ma (SHRIMP U-Pb zircon).|||Is intruded by Kangaroo Creek Supersuite.||
36286|Galloway Volcanic Group|70207|6|Mentioned|p82|||NW of the Newcastle Range.|||||A-type.|
36286|Galloway Volcanic Group|71592|5|Briefly described|Appendix A.||||290+/-3 Ma (SHRIMP U-Pb zircon).||||Dacite.|
34809|Gandry Dam Gneiss|22461|5|Briefly described|Fig 1 p464|||Of the Soldiers Cap Group.||||||15-MAR-07
34809|Gandry Dam Gneiss|22513|6|Mentioned|p373|||Of the Fullarton River Group.||||||19-MAR-18
34809|Gandry Dam Gneiss|22957|6|Mentioned|p133||Statherian|See also Gandry Dam Gneiss Formation.||||||16-MAR-18
34809|Gandry Dam Gneiss|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with the lower sequence of the Georgetown (Qld) Etheridge Group and lower Willyama Supergroup.  (Misspelled usage of Gandry Dam Gneiss Formation)||||||07-NOV-08
34809|Gandry Dam Gneiss|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|||||||
34809|Gandry Dam Gneiss|23972|5|Briefly described|p1427|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier.   Age: 1584 +/- 17Ma.||||||
34809|Gandry Dam Gneiss|24039|6|Mentioned|p457 Fig.2|||||||||
34809|Gandry Dam Gneiss|24253|5|Briefly described|p9|Proterozoic|Proterozoic|Age: ca. 1584 Ma. Geological Province: Mount Isa Block.||||||
34809|Gandry Dam Gneiss|24462|5|Briefly described|p296|||Of the Fullarton River Group.  Geological Province: Mount Isa Block.||||||
34809|Gandry Dam Gneiss|50100|5|Briefly described|p13 Fig.4, p74|Statherian|Statherian|Of the Soldiers Gap Group??  Contains high grade gneisses and iron-rich amphibolites. Geological Province: Eastern Fold Belt Province.||||||
34809|Gandry Dam Gneiss|61929|5|Briefly described|p129 Fig. 3|||Of the Fullarton River Group. See also Lower and Upper Gandry Dam Gneiss. ||||||
34809|Gandry Dam Gneiss|62084|5|Briefly described|p937-938|||Is host succession to Cannington Broken Hill-type deposit occurs in upper amphibolite facies.|max deposit. age 1676+/-5 Ma, Page and Sun 1998||||Interpreted protolith of gneiss (Beardsmore et al. 1998): sandstones, siltstones, volcaniclastic rocks, bimodal volcanic rocks and minor ironstones.|
34809|Gandry Dam Gneiss|63866|5|Briefly described|p63|||According to the authors this is an alternative name for the Soldiers Cap Group in the Cannington area.||||||
34809|Gandry Dam Gneiss|64248|6|Mentioned|p38 Fig.5|Statherian|Statherian||<1676 +/- 5 Ma.|||||11-DEC-17
34809|Gandry Dam Gneiss|64250|6|Mentioned|p7, p11 fig 3, p12-13, p24|||Cloncurry Fold Belt, Mount Isa Inlier. Mis-spelt as Gniess in Fig.7.|<1676 +/- 5 Ma|Fullarton River Group||Is overlain by Glen Idol Schist.||
34809|Gandry Dam Gneiss|65387|6|Mentioned|p84|Statherian|Statherian|Described as a higher-grade equivalent of Soldiers Cap Group.|c.1680-1660 Ma (max. deposition).|||||
34809|Gandry Dam Gneiss|65396|6|Mentioned|p7, p82, p84, p169, p175-178, p195|Statherian|Statherian|See also p197-198, p241, p439. Beardsmore et al. (1988) included this unit in their Fullarton River Group. Isa Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. Detrital zircon sources listed.|<1676 +/- 5 Ma, <1677 +/- 9 Ma|Soldiers Cap Group||Overlain by Llewellyn Creek Formation, Glen Idol Schist.|Upper amphibolite facies rocks.|
34809|Gandry Dam Gneiss|65755|6|Mentioned|p2|||Part of Soldiers Cap Group in the south east, Cloncurry Fault Zone.||||||
34809|Gandry Dam Gneiss|66800|5|Briefly described|p933.|||Felsic. Deposition of its sedimentary precursor between 1676 +/- 5 Ma and 1584 +/- 17 Ma. The former could date contemporary volcaniclastic component; the latter could date high-grade metamorphism.||Unit in Soldiers Cap Group.||||
34809|Gandry Dam Gneiss|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p57|Paleoproterozoic|Paleoproterozoic|Eastern Fold Belt, Mount Isa Inlier. Magnetically-subdued. Asterisked as a redundant rock unit name. Presented as a (former) unit in the Soldiers Cap Group.|1675 +/- 5 Ma (maximum depositional age).|Soldiers Cap Group.|||Psammite-dominated metasedimentary succession.|
34809|Gandry Dam Gneiss|68732|5|Briefly described|p164, p165 Fig.3, p167|Statherian|Statherian|Of the Gun Supersequence. Maximum sedimentary depositional (msed) and igneous crystallisation (ig) ages.|1674+-11,1676+-5,1677+-9 msed; 1678+-5,1689+-13 ig|||||
34809|Gandry Dam Gneiss|73525|6|Mentioned|p4-5 Fig.2|||Snake Creek-Soldiers Cap Domain.|||||Metamorphics.|
24282|Garden Creek Porphyry|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24282|Garden Creek Porphyry|24419|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of Sybella Suite.||||||07-NOV-08
24282|Garden Creek Porphyry|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24282|Garden Creek Porphyry|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24282|Garden Creek Porphyry|37862|4|Described|p585|||||||||
24282|Garden Creek Porphyry|38310|6|Mentioned|p237|||||||||
24282|Garden Creek Porphyry|38350|4|Described|p20|||||||||
24282|Garden Creek Porphyry|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24282|Garden Creek Porphyry|39445|5|Briefly described|Table 2|||||||||
24282|Garden Creek Porphyry|40840|6|Mentioned|Map legend|||||||||
24282|Garden Creek Porphyry|45161|5|Briefly described|p32|||See also p16.||||||05-FEB-07
24282|Garden Creek Porphyry|45166|5|Briefly described|p44|||||||||
24282|Garden Creek Porphyry|46976|6|Mentioned|p98|||||||||
24282|Garden Creek Porphyry|49009|2|Defined|p14|Proterozoic|Proterozoic|Previously mapped as Kalkadoon Granite(Carter & Opik,1963).||||||18-AUG-08
24282|Garden Creek Porphyry|49041|5|Briefly described|Table 1|||||||||
24282|Garden Creek Porphyry|50100|5|Briefly described|p21|Proterozoic|Proterozoic|Of the Sybella Suite.  Comprises massive to locally sheared porphyritic microgranite.  Intrudes the Mount Guide Quartzite.||||||
24282|Garden Creek Porphyry|50536|5|Briefly described|p1.4, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
24282|Garden Creek Porphyry|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic biotite microgranite; minor amphibolite.||||||
24282|Garden Creek Porphyry|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite|||Porphyritic microgranite|
24282|Garden Creek Porphyry|69591|5|Briefly described|p59|||Sybella Batholith.|||||Porphyritic microgranite.|
24282|Garden Creek Porphyry|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain, shown as older than the Isan Orogeny (1590-1500 Ma).||Sybella Suite||Shown as younger than and partially equivalent in age with with Surprise Creek Formation.|Porphyritic microgranite.|
24282|Garden Creek Porphyry|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain, shown as older than the Isan Orogeny (1590-1500 Ma).||Sybella Suite||Shown as younger than and partially equivalent in age with with Surprise Creek Formation.|Porphyritic microgranite.|
35189|Gargett Granite|23042|4|Described|p93,5, Fig 2|Early Permian|Carboniferous|||||||
35189|Gargett Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35189|Gargett Granite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Light grey, fine- to medium-grained, equigranular biotite granite; also light grey, medium-grained hornblende-biotite granodiorite. Part of the Urannah Batholith.||||||
35189|Gargett Granite|65388|2|Defined|p370-371, p135, 362, 364, 365, 380, 389|Early Permian|Late Carboniferous|Northern Connors Arch, Southern Urannah Batholith. Relationships unknown. Two areas of outcrop separated by Pisgah Igneous Complex and Johnston Creek Igneous Complex, so may be older than these units. K-Ar dating of biotite and hornblende gives  ~280-285 Ma  and 295 Ma respectively. Probably minimum ages.  Biotite granite is characteristic, but hornblende diorite, hornblende-biotite granodiorite, hornblende tonalite and porphyritic microgranite are also present.||||||
75122|Garners diorite|60425|5|Briefly described|p62 Tb. 4|Late Ordovician|Ordovician|Informally named subunit of Mission Beach Granite Complex. I-type.||||||07-FEB-11
68998|Garvey Creek Gabbro|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Gabbro and pale grey, slightly porphyritic titanite-bearing hornblende-biotite granodiorite,||||||
40116|Gavial Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbg].  Dark grey medium-grained locally banded hornblende-hypersthene-augite gabbro.||||||
40116|Gavial Gabbro|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
40116|Gavial Gabbro|68008|3|Fully described|p352-355, p361, p621|Early Triassic|Permian|Defined in this study. Gabbro had been noted S and SW of Bouldercombe by Kirkegaard et al. (1970). The type area is along a short section of Gavial Creek, from which it derives its name, S of Bouldercombe township. Has a distinctive high magnetic image. Geophysics modelling. Lack of outcrop conceals relationship with Bundaleer Tonalite.||Bouldercombe Igneous Complex.||Intrudes Capella Creek Group and Mount Alma Formation.|Grey to dark grey, medium-grained gabbro with local compositional banding. Plagioclase laths to 3mm long show crude alignment and comprise over 60% of the rock.|
40116|Gavial Gabbro|68679|5|Briefly described|p424, p426|||Yarrol Province. Eastern lobe of the Complex; part of a gabbroic rim surrounding the core of Bundaleer Tonalite. Hosts gold mineralisation.||Bouldercombe Igneous Complex.||Intrudes Capella Creek Group and Mount Alma Formation.|Hornblende-hypersthene-augite gabbro; irregular, locally banded.|
73612|Gaythorn Metamorphics|67203|5|Briefly described|p6, p9-10 Fig.5, p31|Carboniferous|Carboniferous|Forms basement in eastern Bobby Range area. Appears as Gaythorne Metamorphics in Fig.5 and p9.|||||Low- to medium-grade semi-pelitic and psammitic phyllite and schist.|02-NOV-15
73612|Gaythorn Metamorphics|68319|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Wandilla Province.||||Facies variant of Shoalwater Formation.|Pale grey, fine to medium-grained biotite-muscovite schist, greenish-grey, well-cleaved metasiltstone and pale grey, fine grained quartzose metasandstone.|05-SEP-14
73612|Gaythorn Metamorphics|68421|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province.||||Intruded by the Dahls Hill Complex.|Pale grey, fine to medium-grained biotite-muscovite schist, greenish-grey, well-cleaved metasiltstone and pale grey, fine-grained quartzose metasandstone.|
73612|Gaythorn Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Broome Head and Duckpond Road Metamorphics, Sabina Point Schist, The Shacks Mylonite, Townshend Formation, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
73612|Gaythorn Metamorphics|68679|5|Briefly described|p404, p409|||Wandilla Province. Appears as Gaythorne Metamorphics on p404.|||||Fine- to medium-grained foliated meta-igneous and metasedimentary rocks.|
36253|Geebung Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36253|Geebung Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 284. I-Type.||||||
36253|Geebung Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36253|Geebung Granite|60425|4|Described|p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Fine-grained, granophyric biotite granite. I-type.||||||07-FEB-11
80674|Geikie Granite|71849|3|Fully described|p8, p14, p20,p32, p61-65, p149, p157-158|Devonian|Devonian|See also p21, p195. New name, after the Parish of Geikie. Previously mapped as part of Kintore Adamellite by Trail et al. (1969) and others; resembles the distant Kintore Granite. Small, irregular body c.4.5-8km ~42km N of Coen. Resistant: forms rough hilly country; crops out as tors and large boulders at the type area around MGA 736917 8499318. Geophysics, lithology described. Not isotopically dated; age from similarity to Ebagoola Suite.||Ebagoola Suite.||Adjacent to, and may intrude, Blue Mountains Monzogranite.|White to pale grey, medium-grained, even-grained to slightly porphyritic biotite-muscovite monzogranite. Moderately deformed. High-K calc-alkaline S-type.|10-APR-19
80674|Geikie Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||White to pale grey, medium-grained, even-grained to slightly porphyritic biotite-muscovite monzogranite; moderately deformed.|
23611|Gem Park Granite|42614|6|Mentioned|Table 2 p12|||Reserved.||||||06-MAR-08
23611|Gem Park Granite|42747|5|Briefly described|Fig.9, p38|||see also Table 1 p37.||||||06-MAR-08
23611|Gem Park Granite|43029|2|Defined|p12||Cambrian|see also Fig.2,p16||||||
23611|Gem Park Granite|43204|5|Briefly described|Map Legend|Ordovician|Cambrian|Anakie Inlier||||||23-DEC-11
23611|Gem Park Granite|43213|3|Fully described|p22 Fig.7, p87, p95-98, p104-105, p117|||See also p121-124, p140-143, p175, p179, p208, p211, p214, p231, p240, p243. Rubyvale area. Possibly Cambrian age. Outcrops and type area described. Geochemistry, geophysics, modal analyses and deformation structures detailed. Moderate K and Th anomalies.|375 Ma (Rb-Sr: Carr, pers. comm.,1993).|||Intrudes Bathampton Metamorphics. Is intruded by Whitdale and Mount Newsome Granodiorites, Keilambete Tonalite. Is overlain by Silver Hills Volcanics.|Includes small plutons of variably foliated, cream to pink, fine- to coarse-grained garnet-muscovite-biotite granites. S-type.|
23611|Gem Park Granite|43861|5|Briefly described|25, Fig2p27; p28|||Possibly synchronous with Cambrian metamorphism and deformation.||||||06-MAR-08
23611|Gem Park Granite|68553|6|Mentioned|Map legend|Early Silurian|Ordovician|Anakie Province.||||||
23611|Gem Park Granite|68731|5|Briefly described|p122 Fig 3.10, p130, p133-135|Llandovery|Late Ordovician|Anakie Province. Consists of several elongated intrusions. Zircons from this granite yielded apparent ages of ~2449-302 Ma.|443.3 +/- 6.2 Ma, U-Pb monazite|||Intruded by the Fat Hen Creek Complex and the Mount Newsome Granodiorite.|S-type granite containing biotite and muscovite with quartz, plagioclase, alkali feldspar, and minor garnet.|04-JUL-14
23611|Gem Park Granite|68900|6|Mentioned|p4, p20|Early Silurian|Ordovician|Drummond Basin.||||||
23611|Gem Park Granite|69541|5|Briefly described|p645 Fig.1(b), p654|Early Silurian|Early Silurian|Thomson Orogen.|443 Ma.|||||
23611|Gem Park Granite|70499|5|Briefly described|p5|Earliest Silurian|Earliest Silurian|Geological province: Anakie Inlier, Thomson Orogen. Contains monazite with a mean U-Pb SHRIMP age of 443 Ma (earliest Silurian; Wood, 2006; Wood and Lister, 2013).||||Intruded into Anakie Metamorphic Group; distinct from Retreat Batholith.||
23611|Gem Park Granite|70744|5|Briefly described|p939, p947|||Anakie Province. Associated with Benmabran Orogeny. U-Pb monazite age by Wood and Lister (2013)|443 +/- 6 Ma.|||Intrudes Anakie Metamorphic Group.||
23611|Gem Park Granite|70749|5|Briefly described|p43|Silurian|Silurian|Anakie Province.|443.3 +/- 6.2 Ma.|||||
23611|Gem Park Granite|70856|5|Briefly described|Map Legend|Silurian|Ordovician||||||Cream to pink and grey muscovite and muscovite-biotite granite, commonly strongly foliated and locally mylonitised.|
23611|Gem Park Granite|71966|6|Mentioned|p990|Late Silurian|Late Silurian|Geological province: Anakie Province, Thomson Orogen.|443.3+\-6.2 Ma|||||
23611|Gem Park Granite|73425|6|Mentioned|p16|Silurian|Silurian|Anakie Province, northeast Thomson Orogen.||||||
36164|Giblets Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36164|Giblets Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 265. I-Type.||||||
36164|Giblets Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36164|Giblets Granite|60425|4|Described|p286-7 Appdx. D|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, medium-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
36784|Gibraltar Quartz Monzodiorite|23608|4|Described|p55|||See also page 50, 49 fig.2.  Of Station Creek Igneous Complex. North D'Aguilar Block. Intrudes the Neara Volcanics and Woolooga Granodiorite.||||||
36784|Gibraltar Quartz Monzodiorite|68679|5|Briefly described|p411|Late Triassic|Late Triassic|Tang and Gust (2000). Southern part of the northern New England Orogen. Northern part of Green Rock Quartz Monzodiorite.||Station Creek Igneous Complex.||Contact with Woolooga Granodiorite a net-vein complex.|Leucocratic to quartz monzodiorites.|
28571|Gibsons Gully Aplite|40743|6|Mentioned|p318|||||||||
28571|Gibsons Gully Aplite|41824|6|Mentioned|p201|||||||||
28571|Gibsons Gully Aplite|60425|4|Described|p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Ages: 308Ma, 311+/4Ma (Rb-Sr). White to cream, topaz-bearing aplite. I-type.||||||07-FEB-11
30695|Gidya Granite|50536|5|Briefly described|p8.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30695|Gidya Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite|||Granite|
30695|Gidya Granite|69591|6|Mentioned|p59|||Sybella Batholith.|||||Granite.|
25005|Gilberton Formation|9541|5|Briefly described|Map legend|Carboniferous|Devonian|Cross-bedded pebbly and cobbly arkose with subsidiary conglomerate.||||||19-JUN-13
25005|Gilberton Formation|22744|5|Briefly described|P7, Table2 P9|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|23220|5|Briefly described|Fig.2|Visean|Famennian|Sediment derived from Croydon Volcanic Group. Age: palaeontological - late Famennian to Visean.||||||
25005|Gilberton Formation|23291|3|Fully described|p37, p81 Tb. 3.6|Carboniferous|Devonian|Thickness: 200m. Geological Province: Georgetown Region.||||||08-JUL-15
25005|Gilberton Formation|23430|4|Described|p509 + Plate 14.11|||Gilberton Basin Province.||||||
25005|Gilberton Formation|23495|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|23498|6|Mentioned|p21 table 1|||||||||
25005|Gilberton Formation|23510|5|Briefly described|Map Legend|Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|23513|5|Briefly described|Map legend|Carboniferous|Devonian|Palaeozoic Volcanic No. V10. I-Type.||||||
25005|Gilberton Formation|23619|4|Described|p32 Table 1|Early Carboniferous|Late Devonian|Overlying unit Yellow Jacket Rhyolite - disconformably. Underlying unit Puppy Camp Granodiorite - unconformably.||||||
25005|Gilberton Formation|24013|5|Briefly described|p18 Tb. 1|Early Carboniferous|Late Devonian|Pebble conglomerate, sandstone, arkose, shale.  Correlated with Bundock Creek Formation and part of the Clarke River Formation.  Unconformably overlain by Gilbert River Formation.  Max. thickness: 700ft.||||||
25005|Gilberton Formation|30587|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian to Lower Carboniferous||||||
25005|Gilberton Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
25005|Gilberton Formation|31832|6|Mentioned|Table 6|||||||||
25005|Gilberton Formation|31999|6|Mentioned|Table 11|||||||||
25005|Gilberton Formation|32528|5|Briefly described|Table 1|||||||||
25005|Gilberton Formation|32531|6|Mentioned|p476|||||||||
25005|Gilberton Formation|35811|6|Mentioned|Fig.3|||||||||
25005|Gilberton Formation|35930|6|Mentioned|Fig.1|||||||||
25005|Gilberton Formation|37573|3|Fully described|p212|||See also Figs.2 & 12||||||
25005|Gilberton Formation|37576|5|Briefly described|p8|||||||||
25005|Gilberton Formation|37613|6|Mentioned|p247|||See also Fig.1||||||
25005|Gilberton Formation|38277|6|Mentioned|p154|||||||||
25005|Gilberton Formation|38374|6|Mentioned|p600|||||||||
25005|Gilberton Formation|38714|6|Mentioned|p188|||||||||
25005|Gilberton Formation|39027|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian to Lower Carboniferous||||||
25005|Gilberton Formation|39337|6|Mentioned|Fig.1|||||||||
25005|Gilberton Formation|39445|5|Briefly described|p83|||See also Table 6||||||
25005|Gilberton Formation|39917|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian-Early Carboniferous||||||
25005|Gilberton Formation|41125|6|Mentioned|p42|||||||||
25005|Gilberton Formation|41492|6|Mentioned|Fig.10|||||||||
25005|Gilberton Formation|41675|6|Mentioned|p73|||||||||
25005|Gilberton Formation|42547|3|Fully described|p71|||||||||
25005|Gilberton Formation|43113|4|Described|Table 1 p20|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|43253|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|43259|6|Mentioned|Appendix 1,p2.|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|43461|14|Not recorded|p615|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|43664|6|Mentioned|p80|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|43740|3|Fully described|p5|Visean|Famennian|||||||
25005|Gilberton Formation|44045|14|Not recorded|p154|||||||||
25005|Gilberton Formation|44050|14|Not recorded|p154,158,Pl.2|||||||||
25005|Gilberton Formation|44059|14|Not recorded|p442,445|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|44091|14|Not recorded|p31|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|44516|2|Defined|p33-35|Carboniferous|Late Devonian|Overlain by Blythesdale Group.||||||
25005|Gilberton Formation|44743|14|Not recorded|p40|||Yarrol Basin. Devonian plant fossils.||||||
25005|Gilberton Formation|44800|14|Not recorded|p16,map|Permian|Carboniferous|||||||
25005|Gilberton Formation|45009|2|Defined|p61-2,64,Tb.5,Pl.13|||Unconformably overlies Bernecker Creek Formation. Unconformably overlain by Gilbert River Formation and Agate Creek Volcanics.||||||
25005|Gilberton Formation|46845|6|Mentioned|Table 1|||||||||
25005|Gilberton Formation|50198|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|50199|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Contains the Mamberra Andesite Member.||||||
25005|Gilberton Formation|50210|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
25005|Gilberton Formation|50211|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Lithic to feldspathic sandstone, conglomerate and mudstone.||||||
25005|Gilberton Formation|50595|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes: Spyglass Andesite Member.||||||
25005|Gilberton Formation|60360|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Sandstone, conglomerate and mudstone.||||||
25005|Gilberton Formation|63154|5|Briefly described|p285 Fig. 5|Late Devonian|Late Devonian|Geological province: Georgetown Inlier. Sedimentary rocks.||||||
25005|Gilberton Formation|66529|6|Mentioned|p23 |Devonian|Devonian|||||||
25005|Gilberton Formation|67341|5|Briefly described|p63-65|Early Carboniferous|Early Carboniferous|Georgetown Region, Etheridge Province. Maximum depositional age. Other detrital zircons aged ~1560 Ma are probably sourced from the Forsayth Supersuite and similarly-aged granitic rocks in the region.|~335 Ma (SHRIMP U-Pb zircon).||||Quartzose to feldspathic fluvial sandstones and conglomerates, with sparse tuffs and volcaniclastic sedimentary rocks.|
25005|Gilberton Formation|67430|6|Mentioned|p60, 62, 67|Carboniferous|Devonian|||||Correlated with Maureen Volcanic Group.|Volcanogenic.|
25005|Gilberton Formation|68352|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.|||Includes Spyglass Andesite Member.||Purple to red sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68353|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.|||Includes Mamberra Andesite Member.||Purple to red, brown or green, lithic to feldspathic sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68354|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.|||||Purple to red, brown or green, lithic to feldspathic sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68357|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.|||||Purple to red, brown or green, lithic to feldspathic sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68415|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Gilberton Basin.|||||Purple to red, brown or green lithic to feldspathic sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68477|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Gilberton Basin.|||||Purple to red sandstone, conglomerate and mudstone.|
25005|Gilberton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Gilberton Basin.||||||
25005|Gilberton Formation|68731|5|Briefly described|p187|Mississippian|Late Devonian|Bain et al. (1985). Widespread fluviatile strata across the Georgetown inlier to the west of the Greenvale Province. Palynological data indicate Famennian-Visean (Jell and Playford 1985).||||||
25005|Gilberton Formation|69591|5|Briefly described|p102-103|Visean|Famennian|White (1965). Crops out over ~120 km2 N of the Gilberton Fault in the Gilberton Basin, central Georgetown Inlier. Various occurrences listed. The lower part of this unit contains plant and fish fossils (age implications discussed).|||Mamberra Andesite Member, Spyglass Andesite Member.|Is overlain by Newcastle Range, Cumberland Range, Dismal Creek, Maureen, Volcanic Groups.|Immature and poorly sorted epiclastic sedimentary rocks, mainly quartzose to feldspathic sandstone and polymictic conglomerate; subordinate mudstone and siltstone; a few nodular limestones may be pedogenic, travertine or spring deposits.|
25005|Gilberton Formation|69592|6|Mentioned|p228|Mississippian|Late Devonian|Continental deposits.||||||
25005|Gilberton Formation|70207|6|Mentioned|p14|Early Carboniferous|Late Devonian|Georgetown region.||||||
25005|Gilberton Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|336+/-3 Ma (MDA: U-Pb zircon SHRIMP)||||Ash tuff.|
23616|Gilded Rose Breccia|22460|6|Mentioned|p447|||||||||
23616|Gilded Rose Breccia|22515|6|Mentioned|p401,404,407|||||||||
23616|Gilded Rose Breccia|23971|6|Mentioned|p1408|||Geological Province: Mount Isa Inlier.||||||02-MAR-05
23616|Gilded Rose Breccia|24259|6|Mentioned|p117|||Geological Province: Mount Isa Block. See also Gilded Rose breccias.||||||
23616|Gilded Rose Breccia|41464|6|Mentioned|Map legend|Proterozoic||||||||
23616|Gilded Rose Breccia|41556|6|Mentioned|Map legend|Proterozoic||||||||
23616|Gilded Rose Breccia|41568|3|Fully described|p13|||||||||
23616|Gilded Rose Breccia|41740|6|Mentioned|p222|||||||||
23616|Gilded Rose Breccia|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Breccia.||||||09-FEB-09
23616|Gilded Rose Breccia|43490|6|Mentioned|8|||K-Ar Age: 1488 +/- 11Ma||||||
23616|Gilded Rose Breccia|43616|6|Mentioned|p5|||Age ~1500 Ma||||||
23616|Gilded Rose Breccia|50332|6|Mentioned|p72|||||||||07-FEB-11
23616|Gilded Rose Breccia|61929|6|Mentioned|p135|||||||||
23616|Gilded Rose Breccia|65396|5|Briefly described|p56|Calymmian|Calymmian|Cloncurry district. K-Ar muscovite age of albitization (Perkins and Wyborn, 1998).|1488 +/- 11 Ma.|||||
23616|Gilded Rose Breccia|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p21|Proterozoic|Proterozoic|Soldiers Cap Domain. Calvert Superbasin. Forms small pipe- and dyke-like bodies; may be diatremes.|||||Chaotic polymict breccia derived largely from calc-silicate rocks.|
23616|Gilded Rose Breccia|69056|5|Briefly described|p13|||||Staveley Formation.||||
23616|Gilded Rose Breccia|70353|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic||||||Chaotic polymict breccia derived largely from calc-silicate rocks.|
23616|Gilded Rose Breccia|70354|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic||||||Chaotic polymict breccia derived largely from calc-silicate rocks.|
36985|Gilla Volcanics|23799|3|Fully described|p102, p13 Tb. 1|Triassic|Permian|See als p69 Fig. 5.  Supersedes Gilla Andesite.  Unconformably overlie Maronghi Creek beds and Sugarloaf Metamorphics.  Of the South-east Queensland Volcanic and Plutonic Intrusives.||||||
36985|Gilla Volcanics|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
36985|Gilla Volcanics|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||
36985|Gilla Volcanics|60370|5|Briefly described|Map Legend|Triassic|Permian|Undifferentiated intermediate to acid volcanics.||||||
36985|Gilla Volcanics|68553|6|Mentioned|Map legend|Triassic|Permian|This unit, as well as the Bellthorpe Andesite, the Brookfield Volcanics, and unnamed volcanic units, are all mapped under the symbol, PRv.||||||
36985|Gilla Volcanics|68679|6|Mentioned|p322, p415|Permian|Permian|||||Unconformably overlies Maronghi Creek beds.||
25924|Gilpeppee Member|13497|6|Mentioned|p112|||||Tinchoo Formation|||Coal seams.|
25924|Gilpeppee Member|23375|4|Described|Fig2 p265|Ladinian|Anisian|Of the Tinchoo Formation. In the Cooper Basin.||||||16-APR-08
25924|Gilpeppee Member|42008|2|Defined|p273|Carnian|Ladinian|Reserved as Gilpeppee Formation.||||||
25924|Gilpeppee Member|44133|5|Briefly described|p65 Fig. 8.3|Triassic|Triassic|Of the Tinchoo Formation. Geological Province: Cooper Basin.||||||
25924|Gilpeppee Member|61613|5|Briefly described|p282 Fig. 2|Middle Triassic|Middle Triassic|Of Tinchoo Formation. Underlain by Doonmulla Member. Geological Province: Cooper and Simpson Basins.||||||04-JUL-14
25924|Gilpeppee Member|63978|2|Defined|p25, Fig. 3||Middle Triassic|Upper member of Tinchoo Fm. Conformable on Doonmulla Member (relationship with "upper Doonmulla Mbr.discussed in detail); unconformable under Cuddapan Formation. Max. thickness: 90m. Sequence of dense siltstones with interbedded sandstone and coal.||||||07-FEB-11
25924|Gilpeppee Member|63979|6|Mentioned|p31|||Unconformably overlies the "upper Doonmulla Member"  - both of the Tinchoo Formation.||||||07-FEB-11
25924|Gilpeppee Member|64048|5|Briefly described|p65|||Of the Tinchoo Formation. Relatively uniform sequence of light grey to green-grey, variably carbonaceous siltstones with minor coal development in upper part. May be potential hydrocarbon source rock.||||||07-FEB-11
25924|Gilpeppee Member|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.||Upper unit in Tinchoo Formation.||Overlies Doonmulla Member.||
25924|Gilpeppee Member|65489|6|Mentioned|p96, p131|||Cooper Basin. Could be a potential hydrocarbon source rock.||Unit in Tinchoo Formation.||||
25924|Gilpeppee Member|67402|5|Briefly described|P90 fig CPR4|||Deposited in a fluvial-lacustrine environment. Maximum 100m thick. See also p91 tbl CPR1, p90-p94, p98, p100, p101, p101 tbl CPR2, p105.||Tinchoo Formation||Conformably overlies the Doonmulla Member.|Dense siltstone and mudstone with minor coals and carbonaceous sandstone.|
25924|Gilpeppee Member|68731|5|Briefly described|p200 Fig 3.110, pp208-211|Ladinian|Anisian|Cooper Basin. Powis (1989). ~ 45-100 m thick with Ladinian palynofloras (Gray and McKellar 2002). A palynoflora from high in the Member was assigned to the Late Triassic, but uncertainty remains until it is described.||Of the Tinchoo Formation.||Conformably underlain by the Doonmulla Member. Unconformably overlain by the Cuddapan Formation.|Comprises a relatively uniform succession of carbonaceous siltstones, with interbedded sandstone and coal.|10-MAY-16
25924|Gilpeppee Member|69946|5|Briefly described|p36|Early Triassic|Early Triassic|||Unit in Tinchoo Formation.||Conformably overlies Doonmulla Member. Is overlain unconformably by Cuddapan Formation.||
25924|Gilpeppee Member|70824|6|Mentioned|p104|Middle Triassic|Middle Triassic|Cooper Basin.||Tinchoo Formation||Overlies Doonmulla Member|Dense light grey to green siltstone with minor coal seams and intraclast conglomerate beds.|
25924|Gilpeppee Member|71342|6|Mentioned|Ch5 p36|Carnian|Ladinian|Cooper Basin.  Palynological zone is given in fig 5.3 Ch5 p36.||Tinchoo Formation||||
25008|Gin Gin Basalt|24382|5|Briefly described|Map legend|Eocene|Paleocene|||||||
25008|Gin Gin Basalt|39968|6|Mentioned|p75|||||||||
25008|Gin Gin Basalt|42895|1|Redefined|p52|Paleocene|Late Cretaceous|Excludes older Triassic volcanics of previous definition.||||||18-AUG-08
25008|Gin Gin Basalt|44581|14|Not recorded|p351|||||||||
25008|Gin Gin Basalt|44754|14|Not recorded|Map, p4||Tertiary|||||||
25008|Gin Gin Basalt|61155|5|Briefly described|p20|Early Eocene|Early Paleocene|Together with Pemberton Grange Basalt, overlain by Fairymead beds. In the Bundaberg-Maryborough region. ||||||
25008|Gin Gin Basalt|63821|5|Briefly described|p25, p43|Tertiary|Tertiary|Age: 64.1+/-0.4Ma and 64.7+/-0.3Ma (radiometric K-Ar). Thickness: ~50m. Continental olivine basalt flow.||||||07-FEB-11
25008|Gin Gin Basalt|68332|5|Briefly described|Map legend.|Paleocene|Late Cretaceous|Bundaberg Volcanic Province.|64.7 +/- 0.3 - 64.1 +/- 0.4 Ma.||||Microphyric olivine basalt.|
25008|Gin Gin Basalt|68421|5|Briefly described|Map Legend|Danian|Danian|Bundaberg Volcanic Province. Ages determined from a site on the Childers sheet area.|64.1 +/- 0.4 Ma, 64.7 +/- 0.3 Ma||||Microporphyritic olivine basalt.|20-JUN-13
25008|Gin Gin Basalt|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran and Mount Runsome Basalts; Main Range, Minerva Hills, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
25008|Gin Gin Basalt|69599|5|Briefly described|p645|||Bundaberg area. Whole-rock K-Ar ages by Robertson (1993).|64.7 +/- 0.6 Ma and 64.1 +/- 0.8 Ma.||||Generally tholeiitic lavas.|
25008|Gin Gin Basalt|69600|5|Briefly described|p669|Pleistocene|Pleistocene|Bundaberg area.|||||Vesicular olivine basalt flows.|
32035|Ginger Creek Member|24615|5|Briefly described|CD|Middle Devonian|Middle Devonian|[Dcrg/a].  Andesitic volcaniclastic sandstone.||||||
32035|Ginger Creek Member|50208|5|Briefly described|Map Legend|Devonian|Devonian|Of the Raspberry Creek Formation.||||||
32035|Ginger Creek Member|61730|5|Briefly described|p1001|||Of the Rasberry Creek Formation where the felsic component becomes more extensive.||||||
32035|Ginger Creek Member|68008|3|Fully described|p27,p35,p40-42,p48, p573, p578-579, p601|Middle Devonian|Middle Devonian|Named after Ginger Creek, on western slopes of Ulam Range. Numerous small outcrops; only three mapped. No type section; a type area is a fault block near Ginger Creek. No measured section: thickness estimated at up to a few hundred metres. Forms rugged topography. Shallow-marine (oceanic island-arc) setting. Coral species listed; middle to late Givetian age from conodonts. Close age and composition relationships to Marble Waterhole beds. Micropaleontology table.||Raspberry Creek Formation.||Is unconformably overlain by Balaclava Formation.|Volcaniclastic sandstone, conglomerate and breccia: dacitic and rhyolitic sources; fossiliferous limestone; dacitic and rhyolitic lavas. Local peperite.|
32035|Ginger Creek Member|68679|5|Briefly described|p315-316, p403 Tb.5.8, p425|Givetian|Givetian|Occurs towards the top of the Formation. Covers a relatively large area towards the south. Has lithological and geochemical similarities with Marble Waterhole beds. Age from sparse corals and conodonts.||Raspberry Creek Formation.||Is overlain unconformably by Mount Hoopbound Formation. Is intruded by Cecilwood Quartz Diorite and Bajool Quartz Diorite.|Dacitic and rhyolitic volcaniclastics.|
36236|Gingerella Cauldron Complex|23502|5|Briefly described|Map Legend||Late Carboniferous|Of Sundown Volcanic Group.||||||13-NOV-08
36236|Gingerella Cauldron Complex|23624|6|Mentioned|p18|||||||||
36236|Gingerella Cauldron Complex|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Sundown Volcanic Group.|Includes Double Barrel Andesite, Gingerella Volcanics and Branch Creek Rhyolite.|||
36236|Gingerella Cauldron Complex|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Sundown Volcanic Group.|Includes Double Barrel Andesite, Gingerella Volcanics and Branch Creek Rhyolite.|||
79122|Glanmire Conglomerate Member|70913|4|Described|p24-27, p8 fig 3, p10|Middle Permian|Early Permian|Gympie Province. Discussed as a Member of the Rammutt Formation, but often abbreviated to Glanmire Conglomerate (p20, 23, 24, 26, 27, 67, 77, 79). Replaces the informal Top conglomerate. Named for the Glanmire Gully. Reference drill holes mentioned. A brief description of a type outcrop is also given. Thickness ranges from 10m up to 110m thick. Equated with the Conglomerate Group of Dunstan (1911).||Rammutt Formation||Disconformably or unconformably overlies the Pengelly Siltstone and the Langton Dolerite. Where boundary not a thrust fault, appears to be conformably overlain by the South Curra Limestone.|A coarse-grained, clast-supported, polymictic, volcanoclastic cobble conglomerate with coarse-grained sandstone lenses also present.|18-SEP-17
36323|Glassford Igneous Complex|23468|5|Briefly described|Fig 4 p 298|||||||||
36323|Glassford Igneous Complex|24488|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
36323|Glassford Igneous Complex|24489|5|Briefly described|Map Legend|||||||||
36323|Glassford Igneous Complex|67203|5|Briefly described|p3, p7, p11|Late Triassic|Late Triassic|Despite slightly younger K-Ar ages (Webb and McDougall, 1968), intrusive relationships indicate that these units are marginally older than the Robert Granite (230.2+/-3.7Ma), and therefore broadly contemporaneous with the Bobby Volcanics, Agnes Water Volcanics and other granitoids further east.|||Includes Deception Quartz Monzonite, Rule Gabbro, Lawyer Granite.|Intrudes Bobby Volcanics.|Dominantly high-level (miarolitic and granophyric), leucocratic, alkali-rich granites to quartz monzonites and small gabbro bodies.|12-NOV-15
36323|Glassford Igneous Complex|68008|4|Described|p330, p397-411, p439-460, p493, p529|Triassic|Permian|See also p634-637. Previously the Glassford Complex of Dear et al. (1971). Airborne magnetics and field mapping have resulted in that Complex being subdivided into 13 separate units (2 of which are composite), and renamed Glassford Igneous Complex. Also includes Judas Trachybasalt and Tollbar Breccia.|||Monal, Littlemore Granodiorites; Lawyer, Robert Granites; Rule Gabbro; Deception Quartz Monzonite; Ridler Monzonite; Radley Nepheline Syenite; Burns Spur Nepheline Monzonite. More in Comments.||Monzonite and nepheline syenite.|
36323|Glassford Igneous Complex|68679|5|Briefly described|p338, p428, p431-432, p472|Cretaceous|Late Triassic|A cluster of 13 separate intrusions between Ubobo and Dooloo Tops, New England Orogen.|||Rule Gabbro; Deception Quartz Monzonite; Robert, Lawyer Granites; Littlemore, Monal Granodiorites.||Felsic, leucocratic, granophyric and miarolitic (high-level emplacement); quartz monzonite, granite and granodiorite.|
36323|Glassford Igneous Complex|69594|5|Briefly described|p560-562|||Whitsunday Volcanic Province.|||Burns Spur Nepheline Monzosyenite, Radley Nepheline Syenite, Judas Trachybasalt, Ridler Monzonite.|Intrudes Monal Granodiorite.|Includes granite, rhyolite.|
36323|Glassford Igneous Complex|73450|5|Briefly described|p11, p13-15, p59-66||||||Robert Granite, Ridler Monzonite, Radley Nepheline Syenite, Judas Trachybasalt, Burns Spur Nepheline Monzosyenite|||
80771|Glen Alpine Granite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Pink to brown, medium-grained, slightly to moderately porphyritic, biotite monzogranite; leucocratic; granophyric; with traces of titanite; deeply weathered and poorly exposed.|
80225|Glen Easter Leucogranite|70740|5|Briefly described|p106 fig 62b, p120, p125|Permian|Carboniferous|Distribution and outcrop characteristics briefly discussed on p125. Part of the Kennedy Igneous Association.||||Intrudes Star of Hope Formation. Probably intruded by Easter Granodiorite.|Light pink to grey, leucocratic, fine to medium-grained, equigranular biotite monzogranite; locally miarolitic.|05-OCT-17
74686|Glen Eva Complex|64556|5|Briefly described|p4-17, p55-56|||Age analysis details included (p4-13). Samples analysed include biotite granitic orthogneiss.||||||07-FEB-11
74686|Glen Eva Complex|65452|5|Briefly described|p7 Tb.2|Cisuralian|Cisuralian|SHRIMP U-Pb zircon ages of metamorphism (Carson et al., 2006).|276.8 +/- 4.6 Ma; 274.9 +/- 3.2 Ma.||||Massive to weakly foliated biotite-muscovite tonalitic orthogneiss; migmatitic biotite granitic gneiss.|
74686|Glen Eva Complex|68421|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Coastal Subprovince, Wandilla Province. U-Pb zircon ages (Carson et al. 2006).The minimum age represents a metamorphic age, whilst the maximum age represents a detrital age.|327.6 +/- 3.0 Ma;  274.9 +/- 3.2 Ma|||Intrudes the Tincat Road Metamorphics and the Duckpond Road Metamorphics.|Grey, foliated, fine to medium-grained, slightly porphyritic biotite monzogranite; some intermixed biotite gneiss and migmatitic gneiss.|
74686|Glen Eva Complex|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|||||||
74686|Glen Eva Complex|68679|6|Mentioned|p404|||||||||
74686|Glen Eva Complex|71592|5|Briefly described|Appendix A.|||New England Orogen. Metamorphosed at 275 +/- 3.2 Ma (U-Pb zircon SHRIMP).|||||Migmatite, sedimentary rock.|
74686|Glen Eva Complex|73450|6|Mentioned|p21|||Interpreted to pre-date Borilla Granite.||||||
27272|Glen Garland Granodiorite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
27272|Glen Garland Granodiorite|22781|4|Described|p27|Early Devonian|Early Devonian|Flyspeck Supersuite, ~400Ma||||||
27272|Glen Garland Granodiorite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Two Rail Monzogranite. Age: 398+/-10Ma||||||
27272|Glen Garland Granodiorite|42610|2|Defined|p22|Early Devonian|Early Devonian|Age 398 +/- 10Ma. Unit included in the Flyspeck Granodiorite of B135.||||||
27272|Glen Garland Granodiorite|43738|6|Mentioned|Fig.12,p38|||||||||
27272|Glen Garland Granodiorite|69592|5|Briefly described|p282|||Cape York Peninsula Batholith.|398 +/- 10 Ma (SHRIMP U-Pb zircon).|Flyspeck Supersuite.||||
27272|Glen Garland Granodiorite|71031|5|Briefly described|p2, p26, p29, p32-p33, p36|Devonian|Devonian|Age is a magmatic emplacement age and is also found in Blewett and Trail, 1995.|398 +/- 10 Ma (SHRIMP, Black et al, 1992a, b)|||(Probably) intrudes the Flyspeck Granodiorite.||
27272|Glen Garland Granodiorite|72983|6|Mentioned|p46|||[ambiguous formal or informal use].||||||
27272|Glen Garland Granodiorite|73387|5|Briefly described|p29|Middle Devonian|Early Devonian|Zircon U-Pb (SHRIMP) age of 398 +/- 10 Ma from Black et al. (1992).|398 +/- 10 Ma U-Pb SHRIMP|Flyspeck Supersuite||||20-DEC-22
36259|Glen Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36259|Glen Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 281. I-Type.||||||
36259|Glen Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36259|Glen Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Medium- to coarse-grained porphyritic biotite granite. I-type.||||||07-FEB-11
23619|Glen Idol Schist|22461|5|Briefly described|Fig 1 p464|||Of the Soldiers Cap Group.||||||02-APR-07
23619|Glen Idol Schist|22513|6|Mentioned|p373|||Of the Fullarton River Group. Overlying unit shown as New Hope Arkose.||||||02-APR-07
23619|Glen Idol Schist|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with the lower sequence of the Georgetown (Qld) Etheridge Group and lower Willyama Supergroup.||||||07-NOV-08
23619|Glen Idol Schist|24462|5|Briefly described|p296|||Of the Fullarton River Group.  Geological Province: Mount Isa Block.||||||
23619|Glen Idol Schist|41978|3|Fully described|Table 1 p492|||||||||16-MAR-18
23619|Glen Idol Schist|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Of the Soldiers Gap Group??  Geological Province: Eastern Fold Belt Province.||||||
23619|Glen Idol Schist|61929|5|Briefly described|p129 Fig. 3|||Of the Fullarton River Group. Thickly bedded quartzo-feldspathic psammite with partial melting.||||||
23619|Glen Idol Schist|64250|6|Mentioned|p12-13|||||Fullarton River Group||Overlies Gandry Dam Gneiss.||
23619|Glen Idol Schist|65396|5|Briefly described|p176, p178|||Beardsmore et al. (1988) included this unit in their Fullarton River Group, and correlated it with their New Hope Arkose, a unit they formed from basal Kuridala Formation. Eastern succession, Cover Sequence 3.  ||Fullarton River Group||Overlies Gandry Dam Gneiss. Is correlated with New Hope Arkose.||03-APR-17
23619|Glen Idol Schist|65755|6|Mentioned|p2|||Part of Soldiers Cap Group in the south east, Cloncurry Fault Zone.||||||
23619|Glen Idol Schist|67323|6|Mentioned|Mount Isa Block Time-Space Plot|||Asterisked as a redundant rock unit name. Presented as a (former) unit in the Soldiers Cap Group.||||||
23619|Glen Idol Schist|73525|6|Mentioned|p4-5 Fig.2|||Snake Creek-Soldiers Cap Domain.|||||Metamorphics.|
39105|Glen Oak Diorite|23799|6|Mentioned|p87 Tb. 10|||Informal name of Creaser (1984) for subunit of Eskdale Igneous Complex.  See also "Glen Oak Diorite".||||||
41106|Glen View Quartz Monzodiorite|50301|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
41106|Glen View Quartz Monzodiorite|65388|4|Described|p255-256, p236, 248, 273, 277, 331|Early Permian|Late Carboniferous|Intrudes the Torsdale Volcanics. Inferred to post-date Wind Mill Diorite. Incorporates Boughyard Quartz Diorite, Tan Lies Quartz Monzodiorite of Withnall et al (2007). Interpreted as older than Dawson Granite. Also inferred to pre-date the Ten Mile Granite, Ravenscraig Gabbro. K-Ar isotopic ages: 265 +/-8Ma (hornblende),  290+/-9Ma (biotite) (Whitaker & others, 1974). Mainly pale to dark grey or pinkish grey to pale pink, fine to medium-grained, even-grained to highly porphyritic (mainly plagioclase) quartz monzodiorite, quartz diorite and diorite. Minor gabbro and granodiorite.||||||
41106|Glen View Quartz Monzodiorite|68679|5|Briefly described|p404, p406-408, p419|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Predates or postdates several units listed. K-Ar biotite and K-Ar hornblende ages respectively by Whitaker et al. (1974).|290 +/- 9 Ma and 265 +/- 8 Ma.|||Intrudes Torsdale Volcanics. Is intruded by Ravenscraig Gabbro.|Mainly grey or pinkish, fine- to medium-grained, equigranular to porphyritic (mainly plagioclase) quartz monzodiorite, quartz diorite and diorite, with minor gabbro and granodiorite.|
40122|Glencoe Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRggl].  Gabbro.||||||
40122|Glencoe Gabbro|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
40122|Glencoe Gabbro|60282|6|Mentioned|p22|||||||||
40122|Glencoe Gabbro|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium to coarse-grained, equigranular, melanocratic hornblende-clinopyroxene gabbro, commonly uralitised.||||||
40122|Glencoe Gabbro|65388|5|Briefly described|p315-316, 241, 237, 238, 247, 301, 303|Early Triassic|Late Permian|Rocks mostly previously assigned to Delubra Quartz Gabbro. Some previously included in Glandore Granodiorite. In contact with Kildare, Tandora Granodiorites (probably late Permian to Early Triassic) and Crystal Vale Monzogranite, Mount Clairvoyant, Moocoorooba Granites (Carboniferous). May have caused some recrystallisation in Mount Clairvoyant Granite,  Crystal Vale Monzogranite. Age uncertain. Dominantly medium to coarse-grained, equigranular, melanocratic clinopyroxene-hornblende gabbro. See also p304, 325, 332.||||||
40122|Glencoe Gabbro|68679|5|Briefly described|p408, p410, p416, p419|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Exceptionally large (for this area) mafic intrusion: ~130 km2.||||Probably intrudes Moocoorooba Granite and may intrude Mount Clairvoyant Granite and Crystal Vale Monzogranite. May be intruded by Kildare Granodiorite.|Dominated by medium- to coarse-grained, equigranular melanocratic clinopyroxene-hornblende gabbro; commonly uralitised.|
30539|Glendarriwell beds|23430|5|Briefly described|p510|||||||||
30539|Glendarriwell beds|43204|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||23-DEC-11
30539|Glendarriwell beds|43213|5|Briefly described|p67-69|Early Devonian|Early Devonian|Anakie Inlier. See also Glendarriwell Limestone (p9, p68, p237).||||Correlated with Douglas Creek Limestone and Dunstable Volcanics.|Poorly outcropping limestone, felsic and mafic volcanics, quartzose sandstone and conglomerate.|
30539|Glendarriwell beds|64783|6|Mentioned|p102|Famennian|Famennian|Marine transgression in Emerald area, Drummond Basin.||||||15-NOV-17
30539|Glendarriwell beds|68731|5|Briefly described|p120, p151 Fig 3.51, p177 Fig 3.91, p193|Late Devonian|Late Devonian|Drummond Basin. Veevers et al. (1964b); Jell (1988); Blake, Withnall and Hayward (1995b). Crops out on a small area near Glendarriwell homestead adjacent to the southern margin of the Anakie inlier. Detailed age discussed. See also misspelt Glendariwell beds.|||||Comprises fossiliferous limestone, felsic and mafic volcanics, siltstone, pebbly quartz sandstone and conglomerate.|
30539|Glendarriwell beds|69592|6|Mentioned|p229|Devonian|Devonian|Scattered remnants in central QLD, developed on Thomson Orogen basement.||||||
30539|Glendarriwell beds|70856|5|Briefly described|Map Legend|Early Devonian|Early Devonian||||||Bioclastic limestone (wackestone and packstone), quartzose to lithic sandstone and volcaniclastic conglomerate; minor rhyolite and tuff?|
80226|Glendon Granodiorite|70740|5|Briefly described|p84, p106 fig 62b, p125|Permian|Carboniferous|See also p107, p109, p120, p122. Of Kennedy Igneous Association.||||Intrudes the Smedley Dacite. May be intruded by Charlie Creek Microgranite.|Homogenous light grey, medium-grained, equigranular hornblende, biotite granodiorite.|05-OCT-17
36615|Gleneagle granite|23291|5|Briefly described|p99 Tb. 3.11|Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36615|Gleneagle granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 416.  I-Type.||||||
27782|Glenell Granodiorite|22847|3|Fully described|p 11, 41|||||||||
27782|Glenell Granodiorite|23084|4|Described|p675|Ordovician|Ordovician|||||||
27782|Glenell Granodiorite|23422|6|Mentioned|p209 Table 6.6|||||||||
27782|Glenell Granodiorite|23429|5|Briefly described|Fig 13.25(b) p446|||||||||
27782|Glenell Granodiorite|23504|5|Briefly described|Map Legend||Ordovician|||||||
27782|Glenell Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 104. I-Type.||||||
27782|Glenell Granodiorite|30148|2|Defined|p13|Early Devonian|Late Silurian|Middle Ordovician & Upper Silurian or Lower Devonian.||||||
27782|Glenell Granodiorite|30149|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician and Upper Silurian or Lower Devonian||||||
27782|Glenell Granodiorite|30151|4|Described|Table 1|||Ravenswood Granodiorite Complex.||||||
27782|Glenell Granodiorite|31813|6|Mentioned|Table 2|||Part of Ravenswood. Granodiorite Complex||||||
27782|Glenell Granodiorite|39686|6|Mentioned|p75|||||||||
27782|Glenell Granodiorite|42245|6|Mentioned|p34|||||||||
27782|Glenell Granodiorite|42633|6|Mentioned|Table 1 P8|||||||||
27782|Glenell Granodiorite|43093|4|Described|Appendix 1|||Rb-Sr age of 470+/-30Ma.||||||
27782|Glenell Granodiorite|43259|4|Described|Appendix 1,p22.||Ordovician|||||||
27782|Glenell Granodiorite|43935|5|Briefly described|Map Legend||Ordovician|||||||
27782|Glenell Granodiorite|43936|5|Briefly described|Map Legend||Ordovician|||||||
27782|Glenell Granodiorite|48914|2|Defined|p82|Paleozoic|Paleozoic|See also P21 & 27.||||||07-NOV-08
75730|Glenella Creek Granite|70740|5|Briefly described|p118, p125, p127||||||||Pale pink, medium to coarse-grained, uneven-grained to slightly porphyritic, leucocratic biotite monzogranite.|
70395|Glenelm Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70395|Glenelm Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pink, medium to coarse-grained equigranular biotite granite; minor diorite dykes.|
70395|Glenelm Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, medium- to coarse-grained, equigranular biotite granite; minor diorite dykes.|
70395|Glenelm Granite|73450|6|Mentioned|p16|||||||Intruded by John Clifford Road Granite.||
32146|Glenhalvern Granite|23037|4|Described|p78,9,80|Permian|Silesian|||||||
32146|Glenhalvern Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPggh].  Pink to white, medium- to coarse-grained, biotite granite.||||||
32146|Glenhalvern Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to white, medium- to coarse-grained biotite granite; pink and white, medium- to coarse-grained aplite to microgranite.||||||
32146|Glenhalvern Granite|60282|6|Mentioned|p21|||||||||
32146|Glenhalvern Granite|65388|4|Described|p252-254, p236 Fig. 81, p237, 238,|Early Permian|Late Carboniferous|Inferred to intrude Torsdale Volcanics. Possibly co-magmatic. Unconformably overlalin by  Mount Bulgi Conglomerate Member, Camboon Volcanics. Age from relationships. Relationship with Lonesome Creek Quartz Monzodiorite and Shawlands Granite Complex is unclear. Pink to white, medium to coarse-grained biotite granite||||||
32146|Glenhalvern Granite|68679|5|Briefly described|p404, p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Is overlain unconformably by Mount Bulgi Conglomerate Member (Camboon Volcanics). Is inferred to intrude Torsdale Volcanics. Is intruded by Parraweena Gabbro.|Pink to white, medium- to coarse-grained biotite granite, locally with extensive granophyric intergrowths.|
34819|Glenholme Breccia|22958|6|Mentioned|p125||Proterozoic|Pb-Zn load in lower section of  Cannington deposit Qld.||||||
34819|Glenholme Breccia|23966|6|Mentioned|p1312 Fig. 4|||Geological Province: Mount Isa Inlier.||||||
34819|Glenholme Breccia|50100|6|Mentioned|p69 Fig. 15|||May be the name for a deposit?  Contains siliceous Zn-Pb ore.||||||02-APR-07
27159|Glenidal Formation|22980|5|Briefly described|p255|||||||||
27159|Glenidal Formation|23161|6|Mentioned|p33|||||||||
27159|Glenidal Formation|23430|5|Briefly described|p515|||Of Clematis Group||||||
27159|Glenidal Formation|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Of the Clematis Group.  Age:<241Ma.  Geological Province: Bowen Basin.||||||
27159|Glenidal Formation|35467|6|Mentioned|p180|||||||||
27159|Glenidal Formation|37612|6|Mentioned|Fig.3|||||||||
27159|Glenidal Formation|37804|6|Mentioned|p63|||||||||
27159|Glenidal Formation|38518|6|Mentioned|Fig.3|||||||||
27159|Glenidal Formation|39212|4|Described|p14|||Pedogenesis. See also P36||||||
27159|Glenidal Formation|39445|5|Briefly described|Table 9|||||||||
27159|Glenidal Formation|39491|6|Mentioned|Fig.2|||||||||
27159|Glenidal Formation|39943|6|Mentioned|Table 6A|||||||||
27159|Glenidal Formation|40120|4|Described|p430|||||||||
27159|Glenidal Formation|40999|6|Mentioned|Fig.1|||||||||
27159|Glenidal Formation|41101|6|Mentioned|p295|||||||||
27159|Glenidal Formation|42257|5|Briefly described|Table 1 P263|||||||||
27159|Glenidal Formation|42911|5|Briefly described|p11|||of Clematis Group||||||
27159|Glenidal Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
27159|Glenidal Formation|43185|6|Mentioned|13||Triassic|||||||
27159|Glenidal Formation|43714|6|Mentioned|p33|||||||||
27159|Glenidal Formation|45095|2|Defined|p26|Triassic|Triassic|||||||
27159|Glenidal Formation|62921|6|Mentioned|p878 Fig.2|Early Triassic|Early Triassic|SW Bowen Basin.||||Unconformably overlies Arcadia Formation. Correlated with Clematis Sandstone (Galilee Basin).||
27159|Glenidal Formation|64856|4|Described|p71-75, p102|Anisian|Induan|Jensen (1975). Basal unit of the Clematis Group in Taroom Trough, Bowen Basin. Thin bedded sandstone and lesser siltstone and mudstone. Is overlain by Expedition Sandstone. Palynofloras of APT2 age (251-240 Ma) are associated with this Formation.| | ||||29-NOV-17
27159|Glenidal Formation|64857|4|Described|p126-127|Triassic|Triassic|Thinly bedded, very fine to medium-grained sandstones and common siltstones and mudstones. Appears to be part of the Clematis Group (see text and Fig.3 p113). Base contact appears to be erosional surface.||||||
27159|Glenidal Formation|65115|5|Briefly described|p425, Fig 14 p421|Middle Triassic|Early Triassic|of the Clematis Group, Denision Trough. Underlies the Expedition Sandstone. Part of Supersequence H.||||||
27159|Glenidal Formation|68576|5|Briefly described|Q_4: p16, p21||Early Triassic|Bowen Basin. Meandering stream deposits in a floodplain.||Basal Clematis Group.||Is overlain by Expedition Sandstone.|White to dark brown, very fine- to medium-grained, sub-labile sandstone; lesser grey, mottled brown and red, laminated, micaceous and in part carbonaceous siltstone, and red or red-brown carbonaceous mudstone. Characteristically thin-bedded.|
27159|Glenidal Formation|68679|5|Briefly described|p377, p383|Triassic|Triassic|Jensen (1975). Bowen Basin. 130m thick. Meandering fluvial deposits with palaeosol development.|||||Sublabile sandstone, red to red-brown, yellow-green or grey mudstone, carbonaceous mudstone and brown to red micaceous siltstone.|
32148|Glenleigh Granite|23037|6|Mentioned|p73,4|Permian|Carboniferous|Intrudes the Torsdale Volcanics.||||||
32148|Glenleigh Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPggl].  Pink and white, medium- to coarse-grained, biotite granite.||||||
32148|Glenleigh Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink and white, medium- to coarse-grained biotite granite.||||||
32148|Glenleigh Granite|65388|4|Described|p254-255, p236 Fig. 81, p237, 238, 245|Early Permian|Late Carboniferous|Intrudes the Torsdale Volcanics. Extensive hornfelsing.  Appears to be younger than Glandore Granite. Greyish-white to pink, medium to coarse grained biotite-hornblende granite. Geophysical response compared with Broadlands Granite. Age uncertain. Assumed similar to similar Auburn Arch units.||||||
32148|Glenleigh Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Torsdale Volcanics.|Greyish-white to pink, medium- to coarse-grained biotite-hornblende granite intruded by dacitic to rhyolitic dykes.|
36254|Glenlinedale Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36254|Glenlinedale Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36254|Glenlinedale Granite|60425|4|Described|p285 Appdx., p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Mentioned as being included in Black Prince Granite together with Brownville, Disaster, Stingo and Wilderness Granites on most recent maps. Fine-grained, granophyric biotite granite. I-type.||||||07-FEB-11
80227|Glenmore Creek Granodiorite|70740|5|Briefly described|p126|Permian|Carboniferous|Distribution is briefly discussed. Of Kennedy Igneous Association..||||Probably intrudes the Panhandle Granite and Brawl Creek Granite.|Fine to medium-grained, slightly porphyritic, leucocratic biotite monzogranite with rare sphene.|05-OCT-17
37822|Glenmore Supersuite|23291|3|Fully described|p46, p97 Tb. 3.11|Carboniferous|Carboniferous|||||||
37822|Glenmore Supersuite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Claret Creek, Almaden, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||06-JUN-13
37822|Glenmore Supersuite|69593|4|Described|p484, p488-490|||Mackenzie and Oversby (1997). A small Supersuite (175 km2 outcrop); forms part of the Glenmore Batholith in the southern Georgetown region. Has similarities with Ootann Supersuite. Mineralisation at the (abandoned) Kidston Au mine was genetically related to this unit.|~345-335 Ma (SHRIMP U-Pb zircon ages).||Bagstowe, Lochaber Granites.||(Hornblende-)biotite and biotite granite; locally strongly miarolitic; some accessory topaz and fluorite; local mixing with adjacent mafic rocks. I-type.|
79731|Glennie Creek Granite|71792|2|Defined|p33, p45-p48|Early Permian|Early Permian|Northern Coen Inlier. Named for the Glennie Creek where this unit outcrops. Includes rocks formerly mapped as either Garraway Sandstone or unnamed gabbro/diorite. A type area is proposed at one locality (DPCY062; S 12.5001', E 143.0968'). The unit clearly extends westward beneath the Carpentaria Basin and likely forms a balloon-shaped pluton. Occurs as three small areas of exposure in the northwest of the Coen Inlier. Geophysical characteristics discussed. Appears to be directly overlain by the Garraway Sandstone. Interpreted to intrude the Janet Ranges Volcanics or the Kangaroo River Volcanics. Interpreted to be early Permian in age and part of the Kennedy Igneous Association.|||||Pale grey, fine- to medium-grained, roughly equigranular biotite-hornblende monzogranite.|
79731|Glennie Creek Granite|71853|5|Briefly described|Map legend.|Permian|Permian||||||Pale grey, fine- to medium-grained, roughly equigranular biotite-hornblende monzogranite.|
23621|Glennie Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Wave-dominated deltaic-shallow marine deposits.  Of the Gilbert River Formation.||||||
23621|Glennie Member|42061|5|Briefly described|Fig.4 P159|||||||||
23621|Glennie Member|62837|5|Briefly described|Stratigraphic columns|Valanginian|Berriasian|Of the Gilbert River Formation. Age: ~133-~124Ma. Geological Province: Northern Cape York.||||||01-MAR-10
80772|Glenore Road Quartz Diorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, medium-grained, slightly uneven-grained orthopyroxene-clinopyroxene-hornblende-biotite and clinopyroxene-biotite-hornblende quartz diorite; massive, with mafic inclusions to c. 15 cm across; deeply weathered and poorly exposed.|
33160|Glenprairie beds|60479|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Mainly medium to very coarse grained, moderatly to well sorted feldspatholithic sandstone and conglomerate containing mainly felsic volcanic clasts; subordinate mudstone and siltstone; local felsic volcaniclastic rocks including crystal rich ignimbrite.||||||29-SEP-04
33160|Glenprairie beds|60481|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Mainly medium to very coarse grained, moderatly to well sorted feldspatholithic sandstone and conglomerate containing mainly felsic volcanic clasts; subordinate mudstone and siltstone; local felsic volcaniclastic rocks including crystal rich ignimbrite.||||||29-SEP-04
33160|Glenprairie beds|61035|5|Briefly described|p12|Early Permian|Late Carboniferous|Informal name. Underlain by Tanderra Volcanics. Age: 297Ma (M. Fanning, SHRIMP). Geological Province: Yarrol Province. Consist of feldspath||||||07-FEB-11
33160|Glenprairie beds|65388|3|Fully described|p75-78; p70, 76, 50, 58, 70, 80, 443|Early Permian|Late Carboniferous|Stoodleigh Subprovince, Yarrol Province. New name. Overlies Tanderra Volcanics unconformably. Overlain by or in faulted or thrust contact with Wongrabry beds. Composite, partial type section NW of Bald Hills homestead incorporates the lower part of the Glenprairie beds. Previously mapped as Carmila beds. SHRIMP dating of zircon from an ignimbrite in the Glenprairie beds 297+/-3.6 Ma. May be a correlative of Leura Volcanics, Youlambie Conglomerate. Dominated by feldspatholithic sandstone and lesser conglomerate, siltstone, mudstone and felsic volcaniclastic rocks. See also p445, 446, 447,||||Intruded by Aitken Creek Gabbro, Copperville Granodiorite.||06-SEP-18
33160|Glenprairie beds|68008|6|Mentioned|p132|||||||Possible correlative of Youlambie Conglomerate.||
33160|Glenprairie beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Yarrol Province. This unit, as well as Youlambie Conglomerate and Wongrabry beds, are all mapped under the symbol, CPy.||||||
33160|Glenprairie beds|68679|5|Briefly described|p308, p312-313, p338, p342, p347|Cisuralian|Pennsylvanian|See also p349-350, p359, p426. Withnall et al. (2009). Stoodleigh Subprovince, Northern Yarrol Province. Crops out for ~30km from near Pine Mountain to just S of Charon Point. Strongly deformed: flattened and stretched pebbles and cobbles, slaty cleavage in mudstones, foliation in sandstone and conglomerate. Greenschist metamorphic grade. Probably fluviatile deposits: sporadic plant remains and no marine fossils..|297+/-3.6 Ma (U-Pb zircon: Withnall et al. 2009).|||Is overlain by (locally probably thrust under) Wongrabry beds. Probably equivalent to Youlambie Conglomerate. Is intruded by Aitken Creek Gabbro and Copperville Granodiorite.|Mainly feldspatholithic sandstone (moderately to well sorted felsic volcanic clasts and feldspar) and lesser conglomerate (mostly pebble to cobble clasts of felsic volcanics and intrusives); siltstone, mudstone and felsic volcaniclastics, ignimbrite.|
79944|Glenroy Formation|71965|4|Described|p896,899,903-904,906-908,912-913|Middle Devonian|Early Devonian|Geological province: Thomson Orogen. Observed as a broad area of low and bland magnetic response, consistent with either a monotonous sequence of metasedimentary rocks (e.g. quartz-rich metasandstones), or the presence of a relatively young basin. Lithological constraints provided by scattered drillholes that have intersected low-grade metasedimetnary rocks including quartzite and phyllite. Minimum age provided by intrusion of Scalby Granite dated at 368.4+\-2.3 Ma; effects of possible contact metamorphism represented by slightly elevated magnetic response adjacent intrusion. Proposed to be correlable to Timbury Hills Formation of the Roma Shelf.||||Intruded by Scalby Granite.|Interbedded sandstone and siltstone.|
79944|Glenroy Formation|72522|4|Described|p1-2, p33-40.||Middle Ordovician|Age given is U-Pb SHRIMP maximum deposition age, Purdy et al., 2018. Older detrital zircon components are similar to Thomson beds, but ~460 Ma component distinguishes this unit and may indicate younger deposition. Unit is magnetically bland. Sample is a sand-rich interval within an otherwise mudstone-dominated sedimentary package.|459 +/- 6 Ma 206Pb/238U (204Pb-corrected)||||Fine grained sandstone sampled for dating.  Generally described as low-grade quartzites and phyllites with a single cleavage parallel, or at shallow angle, to bedding.|
78928|Glisson Granodiorite|65388|3|Fully described|p257-258, p236, 243, 247, 251, 253, 276|Late Carboniferous|Late Carboniferous|Auburn Arch. Intrudes Yerilla Metamorphics and is faulted against early Permian Narayen beds. Probably intruded by Jack Shay Gabbro, Sujeewong Gabbro. Relationship with Ah Fat Granodiorite Complex, Evandale Tonalite not known, but age based on similar geophysical character to these units. Separates masses of Dogherty Granite. Brownish grey, medium grained, porphyritic biotite granodiorite to monzogranite in type area.||||||
35543|Gloucester Granite|23162|5|Briefly described|p881||Early Triassic|Age: Zr SHRIMP 243.5+/-4.9Ma.||||||
35543|Gloucester Granite|64570|6|Mentioned|p855|Late Triassic|Late Triassic|Age: 213.5+/-4.9Ma (SHRIMP).||||||22-DEC-08
35543|Gloucester Granite|68358|6|Mentioned|p7|||||||||
35543|Gloucester Granite|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|||||||30-SEP-15
35543|Gloucester Granite|68679|5|Briefly described|p347, p360-361, p364, p365 Fig.5.48|Early Triassic|Early Triassic|See also p367-368. Northern Connors Subprovince, northern New England Orogen. Forms prominent outcrops on Gloucester Island. Texturally and mineralogically heterogeneous, implying the unit is probably composite. Geochemical plots.|243.5 +/- 4.9 Ma (U-Pb SHRIMP: Allen et al., 1998)||||Leucocratic biotite granite with scattered miarolitic cavities and small, vuggy pegmatite patches; relatively mafic hornblende-biotite granodiorite, deformed and partly recrystallised.|
35543|Gloucester Granite|68901|5|Briefly described|p2, p5, p19, p61, p110-p113, p146|Triassic|Triassic|Northern New England Orogen, Bowen Region. SHRIMP ages are interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail. Also 243.5+/-4.9 Ma SHRIMP age from Allen et al., 1998.|243.6 +/- 2 Ma (SHRIMP U-Pb)|||Previously included what is now know to be Cretaceous Horseshoe Bay Granite.|Dated sample: Dark pink, fine- to medium-grained, slightly porphyritic, leucocratic biotite monzogranite. Contains abundant K-feldspar, scattered plagioclase phenocrysts, miarolitic cavitites and vuggy pegmatitic patches.|16-NOV-18
35543|Gloucester Granite|69594|5|Briefly described|p568-571|Early Triassic|Early Triassic|Bowen region. Included in a group of plutons aged <125 Ma. Geochemistry plots and discussion.|||||Dominantly biotite leucogranite.|
35543|Gloucester Granite|69952|6|Mentioned|p85|Triassic|Triassic|||||||
35543|Gloucester Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|244+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
35543|Gloucester Granite|73197|6|Mentioned|p479|Middle Triassic|Middle Triassic||243 Ma U-Pb|||||
24291|Gnallan-a-gea Arkose|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Pebbly arkose, sandstone, siltstone, shale. Overlies: Wonnadinna Dolomite. Underlies: Grant Bluff Formation.||||||28-OCT-04
24291|Gnallan-a-gea Arkose|22649|6|Mentioned|p 152|||Province - Georgina Basin.||||||
24291|Gnallan-a-gea Arkose|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
24291|Gnallan-a-gea Arkose|35863|6|Mentioned|Table 1|||||||||
24291|Gnallan-a-gea Arkose|37928|6|Mentioned|Fig.4|||||||||
24291|Gnallan-a-gea Arkose|41429|6|Mentioned|p247|||||||||
24291|Gnallan-a-gea Arkose|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
24291|Gnallan-a-gea Arkose|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
24291|Gnallan-a-gea Arkose|48990|2|Defined|p11|Adelaidean|Adelaidean|||||||
24291|Gnallan-a-gea Arkose|49027|5|Briefly described|p5|||||||||
24291|Gnallan-a-gea Arkose|61732|6|Mentioned|p108 Fig 40|||Probably partly overlain (in places) by the basal pebbly conglomerate of the Elyuah Formation.||||||07-FEB-11
24291|Gnallan-a-gea Arkose|65338|5|Briefly described|p iv, p63.|Ediacaran|Ediacaran|Probable correlative is recognised in the Boko Formation above the cap dolostone, but not mapped separately in MOUNT PEAKE. Locally interdigitates with Elyuah Formation.||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.||
24291|Gnallan-a-gea Arkose|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Pebbly feldspathic sandstone, siltstone and shale.|
24291|Gnallan-a-gea Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump and Sun Hill Arkoses, Little Burke and Yardida Tillites, are all mapped under the symbol, -P-Cg.||||||
24291|Gnallan-a-gea Arkose|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |More than 1450m thick.||Mopunga Group||Overlain by Grant Bluff Formation|Arkose, sandstone, siltstone and shale.|
24291|Gnallan-a-gea Arkose|73086|6|Mentioned|p118, 122|||Georgina Basin, south-eastern.||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
28006|Go Sam Suite|23291|5|Briefly described|p96 Tb. 3.11|Late Carboniferous|Late Carboniferous|Parent: O'Brien's [misspelling of O'Briens] Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
28006|Go Sam Suite|23423|5|Briefly described|p241||Carboniferous|Age: ~308-315 Ma. O'Briens Creek Supersuite. Kennedy Igneous Province.||||||
28006|Go Sam Suite|23429|5|Briefly described|p441|||||||||
28006|Go Sam Suite|23430|5|Briefly described|p495|||Kennedy Province||||||
28006|Go Sam Suite|23616|5|Briefly described|p75|||Rb-Sr total rock age 313-321 Ma. Also see Table 5 p70. Of O'Briens Creek Supersuite. Coolgarra Batholith.||||||
28006|Go Sam Suite|43060|6|Mentioned|p101|||of O'Briens Creek Supersuite||||||
28006|Go Sam Suite|60425|5|Briefly described|p73, p282-4 Appdx.|||Of O'Briens Creek Supersuite. Includes Go Sam Granite, Askins, Junction, Mount Gibson, Parker and Top Nettle Microgranites, Percy Granophyre, and Pinnacles Granite. I-types.||||||07-FEB-11
28006|Go Sam Suite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.|||I-type.|
24292|Goat Creek Andesite|23291|5|Briefly described|p43, p84, p94|||Of Mount Little Volcanic Group on pages 43 and 94. BUT of Croydon Volcanic Group on page 84 Table 3.6. Geological Province: Georgetown Region.||||||04-JUN-15
24292|Goat Creek Andesite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V800.||||||
24292|Goat Creek Andesite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24292|Goat Creek Andesite|40659|2|Defined|p253|Mesoproterozoic|Mesoproterozoic|Mention P254||||||21-JUN-04
24292|Goat Creek Andesite|40860|4|Described|p110|||||||||
24292|Goat Creek Andesite|40954|6|Mentioned|p132|||||||||
24292|Goat Creek Andesite|41975|6|Mentioned|Fig.3 P433|||||||||
24292|Goat Creek Andesite|43259|4|Described|Appendix 1,p15.||Proterozoic|Age Middle Proterozoic. Of Croydon Volcanic Group.||||||
24292|Goat Creek Andesite|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
24292|Goat Creek Andesite|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24292|Goat Creek Andesite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.|||Amygdaloidal basaltic andesite, commonly agate-bearing, rarely porphyritic; altered.|
24292|Goat Creek Andesite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.|||Amygdaloidal basaltic andesite, commonly agate-bearing, rarely porphyritic; altered.|
24292|Goat Creek Andesite|69591|5|Briefly described|p74 Tb.2.5|||Croydon Province, Georgetown Inlier. 30-100m thick.||Croydon Volcanic Group.|||Amygdaloidal basaltic andesite.|
36425|Goddard Creek Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p29. Kennedy Province.||||||
75726|Goldbeetle Creek Granodiorite|70740|5|Briefly described|p126, p127|||In contact with a number of units (Lizzie Creek Volcanics, Panhandle Granite and Red Hill Creek Granodiorite) though relationships arent given. |||||Grey, fine to medium-grained, moderately porphyritic biotite-hornblende granodiorite to quartz monzodiorite.|
40866|Golden Creek Meta-andesite|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Of the Balcooma Metavolcanic Group.  Meta-andesitic volcaniclastics and lava.||||||
40866|Golden Creek Meta-andesite|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.||Unit in Balcooma Metavolcanic Group.|||Meta-andesitic volcaniclastics and lava.|
40866|Golden Creek Meta-andesite|68731|5|Briefly described|p152, p154|Early Ordovician|Early Ordovician|Comprises a small lens about 2km long. Occurs within the upper part of the Clayhole Schist. Age constrained by the parent Balcooma Metavolcanic Group.||Of the Balcooma Metavolcanic Group.|||Includes mafic volcaniclastic rocks, possible lavas, minor breccia, lithic sandstone and poorly sorted conglomerate containing granules to pebbles of metarhyolite, angular quartz and feldspar.|04-JUL-14
35065|Goldsborough Granodiorite|23049|3|Fully described|p40|Late Silurian|Late Silurian|of Hodgon Suite.||||||
35065|Goldsborough Granodiorite|23283|2|Defined|p23|Devonian|Silurian|||||||
35065|Goldsborough Granodiorite|23422|5|Briefly described|p216 Table 6.10|Late Silurian|Late Silurian|Of Hodgon Suite.||||||
35065|Goldsborough Granodiorite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Hodgon Suite||||||
23624|Goldsmiths Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Part of the Forsayth Supersuite. Geological Province: Georgetown Region.||||||28-MAY-15
23624|Goldsmiths Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 818. S-Type.||||||
23624|Goldsmiths Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|May be misspelt - see also Goldsmith Granite. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
23624|Goldsmiths Granite|37570|4|Described|p119|||||||||
23624|Goldsmiths Granite|38658|6|Mentioned|p152|||||||||
23624|Goldsmiths Granite|39687|6|Mentioned|p3|||||||||
23624|Goldsmiths Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23624|Goldsmiths Granite|41272|5|Briefly described|M 1of1 B05|||||||||
23624|Goldsmiths Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||
23624|Goldsmiths Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
23624|Goldsmiths Granite|50199|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
23624|Goldsmiths Granite|50537|5|Briefly described|p1.2, 1.4, 2.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.||||||
23624|Goldsmiths Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, foliated, medium-grained, variably-porphyritic muscovite-biotite granite with tabular K-feldspar phenocrysts to 2 cm.|
23624|Goldsmiths Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, foliated, medium-grained, variably-porphyritic muscovite-biotite granite with tabular K-feldspar phenocrysts to 2 cm.|
23624|Goldsmiths Granite|68576|6|Mentioned|Q_11: p24|Mesoproterozoic|Mesoproterozoic|Georgetown area.||||||
23624|Goldsmiths Granite|73527|6|Mentioned|p2, p3 Fig.2, p8 Fig.6|||Georgetown Inlier, central domain.||Forsayth Supersuite||||
23624|Goldsmiths Granite|73642|5|Briefly described|p10 Fig.8|Calymmian|Calymmian|Forsayth Batholith.|1551+/-7 Ma|||||
23624|Goldsmiths Granite|75079|5|Briefly described|p3, 5-7, 9-13, 16-18|Mesoproterozoic|Mesoproterozoic|Central domain, Georgetown Inlier. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|1551 +/- 7 Ma.|Forsayth Supersuite.|||Foliated biotite-bearing granite.|
69658|Golliger beds|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlain by Brunette Limestone. Age: <22.5Ma. Thickness: 15m. Geological region: Barkly Tableland.||||||
69658|Golliger beds|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In BAUHINIA DOWNS area. May correlate with Cleanskin beds, Brunette and Austral Downs Limestones.||||||
69658|Golliger beds|69458|5|Briefly described|p42:21|Miocene|Miocene|Northern Barkly Tableland and southern Gulf of Carpentaria regions. Low outcrops. Up to 15m thick. Contains gastropods. Lacustrine deposits. Early to middle Miocene.||||Is overlain by Brunette Limestone.|Massive, white to yellow limestone; grey sandy limestone; contains abundant gastropods.|12-JUL-16
24295|Gongora Granodiorite|23291|4|Described|p48, p98 Tb. 3.11|Permian|Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
24295|Gongora Granodiorite|23430|5|Briefly described|p493|||Kidston Subprovince. Kennedy Province.||||||
24295|Gongora Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 17. I-Type.||||||
24295|Gongora Granodiorite|36216|2|Defined|p210|Mesoproterozoic|Mesoproterozoic|||||||
24295|Gongora Granodiorite|36937|6|Mentioned|p229|||||||||
24295|Gongora Granodiorite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
24295|Gongora Granodiorite|40860|4|Described|p112|||||||||
24295|Gongora Granodiorite|43259|4|Described|Appendix 1,p16.||Permian|Rb-Sr age is 255+/-11 Ma.||||||
24295|Gongora Granodiorite|43664|6|Mentioned|p96||Permian|||||||
24295|Gongora Granodiorite|43740|4|Described|p33||Early Permian|||||||
24295|Gongora Granodiorite|50210|5|Briefly described|Map Legend|Permian|Permian|||||||
24295|Gongora Granodiorite|68415|5|Briefly described|Map Legend|Permian|Permian|Early Permian age. Of the Kennedy Province.|||||Medium to coarse-grained biotite granodiorite with semi-poikilitic K-feldspar phenocrysts.|
24295|Gongora Granodiorite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Western Georgetown region. Unassigned.|||||I-type. Hornblende-biotite and biotite granodiorite (to tonalite), biotite granite; some dolerite.|
35018|Gonyelinka Ignimbrite Member|23037|4|Described|p37|Early Permian|Late Carboniferous|Towards top of Camboon Volcanics.||||||
35018|Gonyelinka Ignimbrite Member|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPvcg].  Rhyolitic to trachytic ignimbrite.||||||
35018|Gonyelinka Ignimbrite Member|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Camboon Volcanics.||||||
35018|Gonyelinka Ignimbrite Member|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Camboon Volcanics.||||||27-MAY-04
35018|Gonyelinka Ignimbrite Member|65388|3|Fully described|p25, p14 Fig. 7, p22 Fig. 10f, p28|||Auburn Arch. Thick ignimbrite. Towards the top of the Camboon Volcanics. The type section is along Lonesome Creek in Gonyelinka Gorge (MGA 218400 7253400 to 218000 7253400), where the unit comprises mainly oligoclase-albite phenocrysts, volcanic lithic fragments in an extremely fine-grained (glassy) matrix containing shards and fiamme. It is ~150m thick. May have vented from Mount Tam. Can be traced ~55km.  Geochem data. Misspelt as Gonyalinka p24. ||||||
35018|Gonyelinka Ignimbrite Member|68679|6|Mentioned|p352|||Auburn Arch, Northern New England Orogen.||||||
75184|Gooburrum Clay|64714|5|Briefly described|p3-4 Fig. 1|Early Miocene|Early Miocene|Conformably overlain by Elliott Formation. Geological province: Bundaberg Trough. Massive pale to medium grey impermeable clay, with minor interbeds of silty sand and carbonaceous clay. ||||||
75184|Gooburrum Clay|68332|5|Briefly described|Map legend.|Miocene|Miocene|Bundaberg Trough. Subsurface only.||||Conformably overlies Fairymead beds. Is overlain conformably by Elliott Formation.|Massive pale to medium grey clay, with minor interbeds of silty sand and carbonaceous clay.|
75184|Gooburrum Clay|68811|6|Mentioned|p50, p51, p162 tbl 25|Tertiary|Tertiary|||||Overlain by the Elliott Formation. Overlies the Fairymead Beds.|Predominantly clay with minor sandy sediments.|
23625|Good Night beds|23251|6|Mentioned|p3, p28|||Previously included in the Gympie Group by Day and others (1978). Of the Gympie Group.||||||21-JUN-06
23625|Good Night beds|24382|5|Briefly described|Map legend|Permian|Carboniferous|||||||
23625|Good Night beds|41736|2|Defined|p115|Early Permian|Carboniferous|||||||
23625|Good Night beds|41738|6|Mentioned|p167|||||||||
23625|Good Night beds|41778|6|Mentioned|Fig.1|||||||||
23625|Good Night beds|42054|6|Mentioned|p273|||||||||
23625|Good Night beds|42895|6|Mentioned|p53|||||||||
23625|Good Night beds|43008|5|Briefly described|map legend|||||||||
23625|Good Night beds|61763|5|Briefly described|p28|||On the MOUNT PERRY 1:100 000 sheets. Limestone/basic volcanics. Geological Province: New England Orogen.||||||
23625|Good Night beds|63821|4|Described|p11, p16|Late Carboniferous|Middle Carboniferous|Geological province: Wandilla Province - Good Night Block. Max. Thickness: >2000m. Sequence of tightly folded, fine-grained metsediments, minor limestone, jasper and volcanics; contain conodonts. In faulted contact with Curtis Island Group.||||||07-FEB-11
23625|Good Night beds|64556|5|Briefly described|p23, p55-56|Late Carboniferous|Late Carboniferous|Ages: 318.7+/-3.0Ma derived from a coherent unimodal zircon population. The unit was affected by metamorphism at 274.9+/-3.2Ma. Age analysis details included. Sample analysed is biotite-garnet meta-psammite.||||||07-FEB-11
23625|Good Night beds|65380|5|Briefly described|p658, p672-673||Late Carboniferous|Coastal Block, New England Orogen. Includes limestone lenses with Late Carboniferous conodonts.||||||27-MAR-12
23625|Good Night beds|68421|5|Briefly described|Map Legend|Permian|Carboniferous|Good Night Subprovince, Wandilla Province. Includes 3 unnamed units, separately mapped.|||||Undivided: slate, phyllite, argillite, chert, jasper, arenite, limestone, basic metavolcanics, diamictite. Separately mapped are hematitic chert or jasper and radiolarian chert; rhyolitic volcaniclastic rocks; andesitic lava and volcaniclastic rocks.|
23625|Good Night beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Coastal Subprovince.||||||
23625|Good Night beds|68679|5|Briefly described|p312-313, p319-321, p324, p369, p420|Pennsylvanian|Pennsylvanian|Cranfield (1989). Previously part of the Biggenden beds of Ellis (1968). Good Night Block, Coastal Subprovince, northern New England Orogen; Wandilla Province accretionary rocks. Exposed over 650 km2. Chert forms prominent N- to NE-trending strike ridges along the western margin. Thickness probably >2000m. Deformation briefly described.||||Is overlain by (?thrust under) Gympie Group. Is faulted against the Curtis Island Group. Correlative of the Bjelke-Petersen beds. Is intruded by Chowey, Mingo Granites and Wateranga Gabbro.|Interbedded slate, phyllite, sandstone, chert and minor limestone and volcanics.|
23625|Good Night beds|72297|5|Briefly described|p708|||Wandilla Province. At Coalstoun Lakes, a significant but subeconomic porphyry copper deposit is associated with diorite-monzonite porphyry stocks and large breccia pipes intruding this unit.|||||Altered sedimentary and volcanic rocks.|
23625|Good Night beds|73450|6|Mentioned|p24|late Carboniferous|late Carboniferous|||||Intruded by Hogback Granite.||
32158|Goodedulla beds|23037|4|Described|p18,24,8,9,48,51,8||Early Permian|||||||
32158|Goodedulla beds|24615|5|Briefly described|CD|Early Permian|Early Permian|[Po].  Predominantly buff, cleaved siltstone and mudstone with lesser volcaniclastic (quartz-poor) sandstone and rare conglomerate.||||||05-SEP-14
32158|Goodedulla beds|50213|5|Briefly described|Map legendperm|Permian|Permian|Predominantly buff, cleaved siltstone and mudstone with lesser volcaniclastic (quartz-poor) sandstone and rare conglomerate.||||||
32158|Goodedulla beds|65388|3|Fully described|p145-146; p174, 34, 48, 70, 108, 121|Early Permian||Connors Arch. Correlated with Woolein Formation. Early Permian? Inferred to overlie Mount Benmore Volcanics and be overlain by Back Creek Group, but may be faults or thrusts. First named and described by Withnall and others (1998a). Adjacent to the Mount Benmore Volcanics over ~30km2 in the Melaleuca Creek area. Yellowish to pale grey cleaved mudstone and siltstone and subordinate volcanolithic sandstone. Lacustrine. Intruded by unnamed gabbro.  See also p125, 174, 176, 338, 447.||||||
32158|Goodedulla beds|68679|5|Briefly described|p308, p353, p355, p360|Permian|Permian|Withnall et al. (1998, 2009). Connors Arch. Occupies a small area N of Rookwood homestead. Deposited in a lacustrine environment in a rift setting. Sediments sourced from underlying Mount Benmore and Leura Volcanics. Unfossiliferous. Early Permian age from stratigraphic position.||Lizzie Creek Volcanic Group.||Overlies Benmore Volcanics. Is thrust against and (probably) overlain by Back Creek Group. Probably correlates with the Woolein Formation and upper part of Carmila beds.|Mainly cleaved siltstone and mudstone; subordinate medium to coarse sandstone and granule to pebble conglomerate, consisting of intermediate volcanic lithic clasts; rare crystal-lithic ignimbrite.|
28271|Goods Island Ignimbrite|23421|4|Described|Table 5.3 p164.||Late Carboniferous|of Torres Strait Volcanic Group. Thickness: +80m. Intruded by Badu Suite.||||||
28271|Goods Island Ignimbrite|32564|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
28271|Goods Island Ignimbrite|33880|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28271|Goods Island Ignimbrite|33883|6|Mentioned|p9|||||||||
28271|Goods Island Ignimbrite|34582|2|Defined|Table 1|Permian|Carboniferous|Carboniferous - Permian||||||
28271|Goods Island Ignimbrite|43567|5|Briefly described|p402|||||||||
28271|Goods Island Ignimbrite|45076|4|Described|p37|||See also p102.  Carb.||||||11-MAY-18
28271|Goods Island Ignimbrite|72983|6|Mentioned|p61|||||Torres Strait Volcanic Group||||
36424|Goold Island Granite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p27. U-Pb SHRIMP 301 +/- 6 Ma. Table 3 p52. Kennedy Province.||||||
36424|Goold Island Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36424|Goold Island Granite|69593|5|Briefly described|p495, p512|Permian|Early Carboniferous|Ingham Batholith. Sm-Nd isotope data tabulated.|301 +/- 6 Ma.||||I-type.|
81007|Goomboorian Igneous Complex|68679|5|Briefly described|p409, p411|Late Triassic|Late Triassic|Northern New England Orogen. Hansen (1997) mapped four lithological groups including a non-cumulate calc-alkaline diorite group and a cumulate hornblende-pyroxene gabbro group. This, and two similar ages, by Green and Webb (1974) are given.|234.8 Ma K-Ar (biotite).||||Diorite, gabbro; reversely zoned, with marginal quartz diorite and hornblende diorite (calc-alkaline) and gabbro core (tholeiitic); magmatic foliation common. M-type affinities. See COMMENTS.|
80773|Goonaneman Road Granite|68679|5|Briefly described|p420-421|Late Triassic|Late Triassic|Gayndah-Gladstone belt. Appears as Gooneneman Road Granite on p420.|||||Biotite hornblende granite.|
27785|Goondicum Gabbro|24488|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
27785|Goondicum Gabbro|24615|5|Briefly described|CD|Late Cretaceous|Late Cretaceous|[Kgoo].  Layered troctolite, olivine-augite gabbro, biotite-hornblende-augite leucograbbro, ferrigrabbro, anorthosite, clinopyroxentie, syentie dykes.||||||
27785|Goondicum Gabbro|30451|4|Described|p84|||Intrudes Lower Palaeozoic rocks||||||
27785|Goondicum Gabbro|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
27785|Goondicum Gabbro|38447|6|Mentioned|Map legend|Triassic|Permian|Permian to Triassic||||||
27785|Goondicum Gabbro|39445|5|Briefly described|Table 12|||||||||
27785|Goondicum Gabbro|50190|6|Mentioned|p28|||Referred to as Mount Goondicum Layered complex in Company Reports.||||||
27785|Goondicum Gabbro|65388|5|Briefly described|p323|||One of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton. May be Cretaceous age.||||||
27785|Goondicum Gabbro|68008|3|Fully described|p435, p460-462|Cretaceous|Cretaceous|Dear et al. (1971). Described as a layered gabbro by Walsh (1972). An almost circular intrusion 6km across, centred c.30km E of Monto. Named after Goondicum homestead. No type area. Forms low undulating country. Geophysics, geochemistry briefly described. Structure described. One of a chain of gabbro intrusions (listed) between Brisbane and Rockhampton. Has been mined for ilmenite and plagioclase.|96 Ma (hornblende: Groen, 1993).|||Intrudes Wandilla Formation.|A lopolithic intrusion with both compositional and igneous layering. Includes olivine gabbro, troctolite, leucogabbro, anorthosite, ferrigabbro, layers rich in magnetite and ilmenite, and marginal hornblende gabbro. Concentric syenite dykes.|
27785|Goondicum Gabbro|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Burns Spur Nepheline Monzosyenite, Judas Trachybasalt, Radley Nepheline Syenite, Ridler Monzonite, Tollbar Breccia, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
27785|Goondicum Gabbro|68679|6|Mentioned|p312|Cretaceous|Cretaceous|Northern New England Orogen.||||||
27785|Goondicum Gabbro|69594|5|Briefly described|p560-562|||Whitsunday Volcanic Province. A distinct circular pluton ~6km in diameter with a distinctive high rim. ~2000m thick. This age is "somewhat uncertain".|96 Ma (Groen, 1993).|||Intrudes Wandilla Formation.|A funnel-shaped, layered, mafic pluton with olivine gabbro, troctolite, leucogabbro, anorthosite, ferrigabbro, magnetite- and ilmenite-rich layers and marginal hornblende gabbro. Is intruded by concentric syenite dykes.|
27785|Goondicum Gabbro|72297|6|Mentioned|p728|||At Goondicum, alluvial, eluvial and floodplain placer deposits (eroded from this unit) contain ilmenite, titanomagnetite, feldspar and apatite.||||||
27785|Goondicum Gabbro|73450|4|Described|p44, p60, p62, p64, p66-69|Cenomanian|Cenomanian|Named by Dear et al. (1971); described by Walsh (1972) and Groen (1993). Crops out as a circular pluton west of Bundaberg, east of Monto. Occurs as a layered pluton with associated dykes. Area underlain by the gabbro is locally referred to as the 'Goondicum crater' and is very prominent on aerial photographs and geophysical images. Forms mainly relatively low undulating country surrounded by a rim of hills of indurated, contact metamorphosed country rocks, with some hilly country towards the centre of the intrusion. Yielded a K-Ar hornblende age of 96 Ma (Groen, 1993).|96 Ma K-Ar|||Intrudes Wandilla Formation and Calliope beds[?].|Includes gabbro, monzodiorite, and peralkaline quartz monzonite.|
34116|Gorge Creek Granite Complex|22630|6|Mentioned|p 3|||||||||
34116|Gorge Creek Granite Complex|22844|6|Mentioned|p41,45,48|||Variation on Gorge Creek Complex,  component of Fat Hen Creek Complex.||||||
34116|Gorge Creek Granite Complex|23049|6|Mentioned|p22|||||||||
34116|Gorge Creek Granite Complex|23422|5|Briefly described|p174|||Originally thought to intrude the Fat Hen Creek Complex, this relationship is now uncertain.||||||
36388|Gorge Creek Suite|23422|4|Described|p211 Table 6.7|||||||||
36388|Gorge Creek Suite|23430|5|Briefly described|480p|Ordovician|Mesoproterozoic|Significance of magmatic zircon age 1105+/-15 Ma, complex zircon age 1238 +/-38 Ma is uncertain. Considered part of Early Ordovician Fat Hen Creek Complex.||||||13-JAN-05
36388|Gorge Creek Suite|23431|5|Briefly described|p537|||||||||
36388|Gorge Creek Suite|68731|5|Briefly described|p147|Early Ordovician|Series 3|Contains zircons interpreted as magmatic yielded 1105 +/- 15 Ma and 1238 +/- 38 Ma ages, but the significance of these ages remains unclear.|493 +/- 10 Ma||||Hornblende-bearing granitoid.|
31678|Gorge Quartzite|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
31678|Gorge Quartzite|22781|4|Described|p21|Proterozoic|Proterozoic|Holroyd Group||||||
31678|Gorge Quartzite|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group, Coen Inlier. Thickness 3000m||||||
31678|Gorge Quartzite|23431|5|Briefly described|p535|||of Holroyd Group.||||||
31678|Gorge Quartzite|43596|4|Described|p19 Tb. 1, p23|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group. Max. thickness: 1300m.Intruded by Cape York Batholith. Fine- to med.-gr., muscovite quartzite interlayered with sillimanite-muscovite-quartz schist; andalusite, local garnet and graphite.||||||05-NOV-08
31678|Gorge Quartzite|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||
31678|Gorge Quartzite|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. 1300m thick. Occurs mostly between Lukin and Holroyd Rivers; some around Coleman River. Linear ridges of quartzite are characteristic.||Holroyd Group.|||Thick-bedded muscovite quartzite, sillimanite-mica schist. Becomes more pelitic to the east.|
31678|Gorge Quartzite|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|The two facies are mapped separately.||Holroyd Group.||Partly interlayered with Gorge Quartzite.|Medium-grained quartzite with muscovite, biotite, hematite, garnet in places. Muscovite quartzite, sillimanite-muscovite-quartz schist; andalusite, graphite or garnet locally.|
36423|Gorge Range Microgranite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|SHRIMP 301 Ma. Intrude Wallaman Falls Volcanics. Also see p26. Kennedy Province.||||||
36423|Gorge Range Microgranite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36423|Gorge Range Microgranite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
27423|Gotthardt Granodiorite|23052|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
27423|Gotthardt Granodiorite|23161|4|Described|p47 table6|Early Cretaceous|Early Cretaceous|Ages: 119.7+/-27Ma & 118.6+/-7.4 Ma.||||||
27423|Gotthardt Granodiorite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
27423|Gotthardt Granodiorite|32553|4|Described|p56|||||||||
27423|Gotthardt Granodiorite|34314|6|Mentioned|p12|||||||||
27423|Gotthardt Granodiorite|37458|6|Mentioned|p435|||||||||
27423|Gotthardt Granodiorite|39445|5|Briefly described|Table 12|||||||||
27423|Gotthardt Granodiorite|41246|6|Mentioned|Map legend|Cretaceous||||||||
27423|Gotthardt Granodiorite|42701|4|Described|p101|||||||||
27423|Gotthardt Granodiorite|43988|14|Not recorded|Map Legend||Early Cretaceous|||||||
27423|Gotthardt Granodiorite|44001|14|Not recorded|Map Legend||Mesozoic|||||||
27423|Gotthardt Granodiorite|44245|5|Briefly described|Map Legend||Cretaceous|||||||
27423|Gotthardt Granodiorite|48841|14|Not recorded|p31,43,47|||Occupies core of dome in Upper Bowen Coal Measures.||||||
27423|Gotthardt Granodiorite|65388|5|Briefly described|p406|||Intrudes Bowen Basin, along with Mount Barker Granodiorite, and Bundarra Granodiorite further east. All have also produced metamorphic aureole in surrounding sediments too. ||||||
27423|Gotthardt Granodiorite|69760|6|Mentioned|p140 Fig.2|||Hail Creek, Bowen Basin.||||||
27423|Gotthardt Granodiorite|73037|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Biotite hornblende granodiorite.|
27423|Gotthardt Granodiorite|73038|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Biotite hornblende granodiorite.|
24300|Gowers Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Middle Cambrian|||||||
24300|Gowers Formation|40386|6|Mentioned|p429|||||||||
24300|Gowers Formation|40686|2|Defined|p409|Middle Cambrian|Middle Cambrian|||||||
24300|Gowers Formation|40852|5|Briefly described|p39|||||||||
24300|Gowers Formation|40855|6|Mentioned|p329|||||||||
24300|Gowers Formation|40954|6|Mentioned|p133|||||||||
24300|Gowers Formation|41240|6|Mentioned|p126|||||||||
24300|Gowers Formation|47058|5|Briefly described|p125|||||||||
24300|Gowers Formation|64068|6|Mentioned|p59, 225|||Of Southgate (1986).||||Disconformably overlies Thorntonia Limestone.||21-MAR-16
24300|Gowers Formation|64443|6|Mentioned|p40|||Correlative of Wonarah Formation.||||||
24300|Gowers Formation|65337|6|Mentioned|p65.|||Consists of former basal beds of the Currant Bush Limestone in CAMOOWEAL area, renamed by Southgate (1986).||||||
24300|Gowers Formation|67352|6|Mentioned|p69|||||||||
24300|Gowers Formation|69443|5|Briefly described|p28:16, 20, 22-23|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Disconformably overlies Thorntonia Limestone. Is overlain disconformably by Currant Bush Limestone. Correlated with Anthony Lagoon, Wonarah Formations.||12-JUL-16
24300|Gowers Formation|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
24300|Gowers Formation|69591|4|Described|p88-89, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Formerly included in the basal part of Currant Bush Limestone. Separately defined by Southgate (1986) as an arc from 8km S of Gowers Bore to Plumtree Bore. Is 6.3m thick at the type locality, a few hundred metres S of Gowers Bore. Supersedes (and includes much of) the Chummy Bore Formation (deKeyser, 1973). Richly fossiliferous.||Narpa Group.||Paraconformably overlies Bronco Stromatolith (Thorntonia Limestone). In part equivalent to Inca Formation.|Oolitic.|
24300|Gowers Formation|72321|6|Mentioned|Fig 2|Wulian|Wulian|Undilla Sub-basin, Georgina Basin. Australian Stage: Templetonian. ||of Narpa Group.||||
24300|Gowers Formation|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Underlies Currant Bush Limestone|Phosphorite.|
36422|Gowrie Creek Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p27. Intrudes Wallaman Falls Volcanics and Rockingham Bay Granite. Kennedy Province.||||||
36422|Gowrie Creek Granodiorite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36422|Gowrie Creek Granodiorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
29610|Gowrie Suite|43005|5|Briefly described|p215|||||||||
40123|Gracemere Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbr].  Grey medium- to coarse-grained foliated quartz-hornblende-biotite-hypersthene-augite gabbro.||||||
40123|Gracemere Gabbro|50208|5|Briefly described|Map Legend|Triassic|Permian|||||||
40123|Gracemere Gabbro|50209|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
40123|Gracemere Gabbro|50212|5|Briefly described|Map Legend|Early Triassic|Late Permian|Of Bouldercombe Igneous Complex.||||||14-MAY-04
40123|Gracemere Gabbro|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
40123|Gracemere Gabbro|60557|5|Briefly described|p32|||Part of the Bouldercomb Complex (ie. the Bouldercombe Igneous Complex)..||||||09-JUN-05
40123|Gracemere Gabbro|68008|2|Defined|p335, p355-357, p359, p361, p366, p621|Early Triassic|Permian|Named after the Parish and township of Gracemere. The type area is a series of decomposed granite pits 3km SE of Gracemere, the largest of which is the local rubbish dump. Forms an arcuate belt 10 x 3 km SE from Gracemere. Geophysics briefly described and modelled. K-Ar biotite age (recalculated) conflicts with the Late Permian age of the Bundaleer Tonalite, which is interpreted to intrude the Gabbro. Hosts the Hector gold mine.|244 +/- 5 Ma (Webb and McDougall, 1968).|Bouldercombe Igneous Complex.||Intrudes Rockhampton Group. Is intruded by Kabra Quartz Monzodiorite and (probably) Bundaleer Tonalite.|Uniform, grey, medium- to coarse-grained gabbro with a prominent foliation due to alignment of plagioclase laths. Foliated during emplacement.|
40123|Gracemere Gabbro|68679|4|Described|p424, p426|||Yarrol Province. An arcuate belt ~10 x 3km along the northeastern lobe of the Complex; part of a gabbroic rim surrounding the core of Bundaleer Tonalite.|244 +/- 5 Ma (K-Ar: Webb and McDougall, 1968).|Bouldercombe Igneous Complex.||Intrudes Rockhampton Group. Is intruded by Bundaleer Tonalite and Kabra Quartz Monzodiorite.|Foliated quartz-hornblende-biotite-hypersthene-augite gabbro.|
25933|Grahams Creek Formation|22857|5|Briefly described|p310|Early Cretaceous|Early Cretaceous|Geological Province: Maryborough Basin.||||||
25933|Grahams Creek Formation|22865|6|Mentioned|p310||Early Cretaceous|||||||
25933|Grahams Creek Formation|23277|6|Mentioned|p59|||(Ellis, 1968).||||||
25933|Grahams Creek Formation|23841|4|Described|p448|Early Cretaceous|Early Cretaceous|Geological Province: Maryborough Basin.  Maximum thickness: ~1220m.||||||
25933|Grahams Creek Formation|23911|6|Mentioned|p86|||Geological Province: Maryborough Basin.||||||
25933|Grahams Creek Formation|24382|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
25933|Grahams Creek Formation|29651|6|Mentioned|Fig.1|||See also P1||||||
25933|Grahams Creek Formation|30654|4|Described|p50|||See also P51,53,55,56,59. Neocomian age||||||
25933|Grahams Creek Formation|30655|3|Fully described|p21|||See also Table 1.||||||26-MAR-15
25933|Grahams Creek Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
25933|Grahams Creek Formation|32137|5|Briefly described|p355|||Age||||||
25933|Grahams Creek Formation|32774|5|Briefly described|Table 2|||||||||
25933|Grahams Creek Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
25933|Grahams Creek Formation|33349|6|Mentioned|p687|||||||||
25933|Grahams Creek Formation|34408|6|Mentioned|p190|||Lower Cretaceous||||||
25933|Grahams Creek Formation|35101|6|Mentioned|p94|||||||||
25933|Grahams Creek Formation|35813|6|Mentioned|p581|||||||||
25933|Grahams Creek Formation|35937|6|Mentioned|Fig.5|||||||||
25933|Grahams Creek Formation|36575|6|Mentioned|Fig.1|||||||||
25933|Grahams Creek Formation|36926|6|Mentioned|p173|||See also P176.||||||
25933|Grahams Creek Formation|36961|6|Mentioned|Table 1|||||||||
25933|Grahams Creek Formation|37118|6|Mentioned|p317|||||||||
25933|Grahams Creek Formation|37120|6|Mentioned|Fig.2|||||||||
25933|Grahams Creek Formation|37618|4|Described|p26|||||||||
25933|Grahams Creek Formation|37861|6|Mentioned|p591|||||||||
25933|Grahams Creek Formation|38309|6|Mentioned|p227|||||||||
25933|Grahams Creek Formation|38397|4|Described|Table 2|||||||||
25933|Grahams Creek Formation|38398|6|Mentioned|p54|||||||||
25933|Grahams Creek Formation|39211|5|Briefly described|p41|||See Fig. 25.||||||
25933|Grahams Creek Formation|39315|6|Mentioned|Fig.5|||||||||
25933|Grahams Creek Formation|39445|5|Briefly described|Table 10|||||||||
25933|Grahams Creek Formation|39505|6|Mentioned|p167|||||||||
25933|Grahams Creek Formation|39968|6|Mentioned|p80|||||||||
25933|Grahams Creek Formation|40245|6|Mentioned|Fig.4|||Mention Table 1||||||
25933|Grahams Creek Formation|41265|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
25933|Grahams Creek Formation|41736|6|Mentioned|Fig.1|||||||||
25933|Grahams Creek Formation|41738|6|Mentioned|p174|||||||||
25933|Grahams Creek Formation|42075|5|Briefly described|Fig.18 P256|||||||||
25933|Grahams Creek Formation|42616|4|Described|p7|||||||||
25933|Grahams Creek Formation|42636|5|Briefly described|p9|||||||||
25933|Grahams Creek Formation|42894|2|Defined|p26|Early Cretaceous|Late Jurassic|See also Fig.2 p22.||||||26-MAR-15
25933|Grahams Creek Formation|42895|5|Briefly described|p51|||||||||
25933|Grahams Creek Formation|43008|5|Briefly described|map legend|||||||||
25933|Grahams Creek Formation|43059|4|Described|Table 1|||see also p9||||||
25933|Grahams Creek Formation|44068|14|Not recorded|p15|||||||||
25933|Grahams Creek Formation|44082|6|Mentioned|Table p34||Neocomian|Mention on correlation table of Queensland sediments.||||||
25933|Grahams Creek Formation|44091|14|Not recorded|p63||Cretaceous|||||||
25933|Grahams Creek Formation|44762|14|Not recorded|Map||Cretaceous|||||||
25933|Grahams Creek Formation|44786|14|Not recorded|p193-202||Early Cretaceous|||||||
25933|Grahams Creek Formation|44821|14|Not recorded|p33,34,38|Early Cretaceous|Late Jurassic|||||||
25933|Grahams Creek Formation|45107|6|Mentioned|p6|||||||||
25933|Grahams Creek Formation|45440|4|Described|p.2,14,29,31,32-68|||Tb.1. Of many pages. ?Neocomian||||||
25933|Grahams Creek Formation|60281|5|Briefly described|p37, Fig. 30 App.1|Early Cretaceous|Late Jurassic|Intermediate to acid flows and pyroclastics, tuffaceous sandstone, siltstone.  Unconformably overlies the Duckinwilla Group; Underlies the Maryborough Formation.  Age: 140+/-5Ma. for an andesite flow near Maryborough (K-Ar).  Max. thickness: 1200m.||||||
25933|Grahams Creek Formation|62594|5|Briefly described|p545, p546 Fig. 3|Early Cretaceous|Jurassic|Tuffs, agglomerates and volcanic breccias overlain by trachyte and rhyolite flows, overlain by basaltic andesite and dacite. Age: largely Neocomian. Geological Province: Maryborough Basin. See also p559.||||||09-AUG-06
25933|Grahams Creek Formation|63821|4|Described|p22, p23|Cretaceous|Jurassic|Unconformably overlies Tiaro Coal Measures. Intruded by Mount Bauple Syenite. Geological Province: Maryborough Basin. Comprises intercalated volcanics (trachyandesite, andesite and trachyte flows) and minor volcaniclastic sediments. See also p37.||||||07-FEB-11
25933|Grahams Creek Formation|64570|6|Mentioned|p858|||||||||
25933|Grahams Creek Formation|64665|6|Mentioned|p53 Fig.2.|Early Cretaceous|Early Cretaceous|Northern Nambour and Maryborough Basins.||||||
25933|Grahams Creek Formation|64714|6|Mentioned|p9|||||||||
25933|Grahams Creek Formation|65107|6|Mentioned|p295|Early Cretaceous|Late Jurassic|145-136 Ma||||||
25933|Grahams Creek Formation|67402|4|Described|p234, p235, p236|Valanginian|Oxfordian|Maryborough Basin. Deposited in a continental and lacustrine environment. ||||Unconformably overlies the Tiaro Coal Measures. Unconformably overlain by the Gregory Sandstone.|Intermediate to acidic flows and pyroclastics, tuffaceous sandstone and siltstones.|
25933|Grahams Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Maryborough Basin.||||||
25933|Grahams Creek Formation|68679|6|Mentioned|p312-313, p435|Early Cretaceous|Jurassic|Northern New England Orogen.||||||
25933|Grahams Creek Formation|69582|5|Briefly described|p48, p50, p53|Early Cretaceous|Early Cretaceous|Maryborough Basin. Thermal conductivity is provided. Intersected in GSQ Maryborough 16.||||Unconformably overlies the Tiaro Coal Measures. Unconformably overlain by the Maryborough Formation and the Burrum Coal Measures.|Rift related volcanic rocks including andesite.|
25933|Grahams Creek Formation|69594|4|Described|p519, p548-549, p552|Early Cretaceous|Early Cretaceous|Hawthorne (1960); Cranfield (1993). Maryborough Basin. Part of the Whitsunday Volcanic Province. Rift-related, bimodal, terrestrial, interbedded volcanics and volcaniclastic sedimentary rocks (mostly fluvial) and hypabyssal intrusions. Up to ~1200m thick in the type section on the Maryborough to Brooweena road (Ellis, 1968). Strata are generally flat-lying but locally have steep dips or are overturned. Lithologies described in some detail. Berriasian-Valanginian. Geochronology by Green and Webb (1974): other age determinations discussed. An exploration target for epithermal precious metal mineralisation.|140 +/- 5 Ma : whole-rock K-Ar (andesite).|||Unconformably overlies Tiaro Coal Measures and Brooweena Formation. Is overlain disconformably/unconformably by Maryborough Formation.|Rhyolitic lavas and ignimbrites, microdiorite to microgranodiorite to granite, coarse-grained volcanic breccia; feldspathic-volcanic lithic sandstone, siltstone, volcanogenic polymict conglomerate; carbonaceous shale and mudstone at the top.|
25933|Grahams Creek Formation|69599|5|Briefly described|p610|||Correlated with volcanic rocks at the bottom of drillholes in the Capricorn Channel (offshore Maryborough Basin).||||||
25933|Grahams Creek Formation|73422|5|Briefly described|p1-9|Valanginian|Berriasian|Maryborough Basin. Morton Igneous Association. [Also written as Graham's Creek Formation]. Constitutes the basal unit of the basin. New U-Pb zircon age of 139.9 +/- 0.7 Ma. Whole rock K-Ar ages of 140 +/- 5 Ma, 101 +/- 5 Ma were reported by Cranfield (1993, 1994). Maximum thickness of 1200 m (Cranfield, 1993). Also widely distributed across the offshore sector of the basin where it is up to 3 km thick (Hill, 1994).|139.9 +/- 0.7 Ma U-Pb zircon|||Overlain by Maryborough Formation. Underlain by Tiaro Coal Measures.|Intermediate to silicic volcanic to volcaniclastic rocks of basaltic to dacitic composition. Includes basaltic tuffs and lava flows, and andesitic to dacitic volcanic breccias and tuffs.|
78569|Granite Springs Granite|68731|5|Briefly described|p166 Fig 3.78, p167, p167 incl. Tb 3.2|Late Ordovician|Middle Ordovician|S-type(?) granite. Uncertain whether youngest zircons indicate emplacement age of the granite or represent inherited grains. See also Eulo Ridge Granite.|456.3 +/- 3.9 Ma (U-Pb zircon).||||Comprises grey, fine- to medium-grained, porphyritic muscovite-biotite monzogranite.|04-JUL-14
78569|Granite Springs Granite|68901|5|Briefly described|p5|||Upper Ordovician?|||||Grey, porphyritic muscovite-biotite monzogranite.|
78569|Granite Springs Granite|69952|5|Briefly described|p1, p2 Tb.i, p15-29|Late Ordovician|Late Ordovician|Northern part of the Eulo Ridge, Thomson Orogen. Forms numerous large boulders, and scattered whalebacks and pavements. SHRIMP U-Pb zircon age of emplacement; other ages given.|455.6 +/- 5.4 Ma (Cross et al., 2015).||||Includes grey, porphyritic muscovite-biotite monzogranite, extensively deformed and partly recrystallised; fine-grained granodiorite, and diorite.|
78569|Granite Springs Granite|70499|6|Mentioned|p3,6-7|Late Ordovician|Late Ordovician|Geological province: Anakie Inlier, Thomson Orogen. Analysis of 2 zircons yield (U-Th)/He ages 255 and 356 Ma, and U-Pb SHRIMP age of 456.3+\-3.9 Ma (Cross et al., 2015).||||||
78569|Granite Springs Granite|70720|4|Described|p1-28|Ordovician|Ordovician|Eulo Ridge, southern Thomson Orogen. Occurs as discrete, steep-sided masses surrounded and locally onlapped by overlying Eromanga Basin units. Relatively bland magnetic zone within and distinct from the strong Werewilka formation fabric. Mineralogy, geochemistry discussed in some detail; geochronology/thermochronology and textures in great detail.|455.6 +/- 5.4 Ma (SHRIMP U-Pb zircon).|||Is overlain nonconformably by Doncaster Member and Winton Formation.|S-type, locally coarsely porphyritic, biotite-muscovite syenogranite with common igneous and metasedimentary inclusions; locally characterised by abundant, moderately to strongly aligned large alkali feldspar phenocrysts. Pegmatite dykes and pods.|
78569|Granite Springs Granite|70744|5|Briefly described|p939|||Thomson Orogen (NW NSW). Age by Bultitude and Cross (2013).|c.455 Ma (estimated from Fig.7).|||||
78569|Granite Springs Granite|70749|5|Briefly described|p43|Ordovician|Ordovician|Southern Thomson and Koonenberry area.|456.3 +/- 3.9 Ma.|||||
78569|Granite Springs Granite|70821|5|Briefly described|p9-10, p12, p13 Tb.2.1, p87|Late Ordovician|Middle Ordovician|Highly resistive.|456.3 +/- 3.9 Ma (Bultitude and Cross, 2013).||||Includes monzogranite.|01-DEC-16
78569|Granite Springs Granite|71251|6|Mentioned|p3|||Yowah-Cunnamulla area.||||||
78569|Granite Springs Granite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|456+/-5.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite, monzogranite.|
78569|Granite Springs Granite|71860|5|Briefly described|p7|||Age is a SHRIMP U-Pb date.|456.3 +/- 3.9 (Bultitude et al. 2012)||||Monzogranite.|
78569|Granite Springs Granite|71864|6|Mentioned|p3|||||||||
78569|Granite Springs Granite|71965|5|Briefly described|p897,906-909,912-913|Late Ordovician|Late Ordovician|Geological province: Thomson Orogen. Outcropping S-type granite in the southern Thomson Orogen. Remnants of Werewilka Formation occur as biotite schist and quartz xenoliths in Granite Springs Granite. Dated at 455.6+\-2.4 Ma (Cross et al., 2015).|455.6+\-5.4 Ma||||Coarsely porphyritic, foliated, biotite-muscovite alkali feldspar granite to monzogranite with metasedimentary inclusions, shear zones (sinistral) and pegmatitic veins, dykes and pods.|
78569|Granite Springs Granite|71966|6|Mentioned|p990|Late Ordovician|Late Ordovician|Geological province: southern Thomson Orogen.|456.3+\-3.9 Ma|||||
78569|Granite Springs Granite|72522|4|Described|p2, p5 Tb.1.1, p49-53, p147.|Late Ordovician|Middle Ordovician|U-Pb zircon SHRIMP magmatic crystallisation age for granite from Cross et al., 2015. Xenolith dated by same method herein. Interpretation confirmed by 453.1+/-6.4 Ma date from  monazite from the same sample in 2015. One of very few exposed granites in the southern Thomson Orogen. Crops out along Eulo Ridge north of Currawinya and Hungerford Granites.|455.6+/-5.4 Ma. 454.5 +/- 4.3 Ma (xenolith)||||Includes metasedimentary xenoliths and mafic enclaves.|
78569|Granite Springs Granite|73600|6|Mentioned|p203|Late Ordovician|Late Ordovician|Eulo Ridge.||||||
75627|Grant Creek Granite|68679|5|Briefly described|p363, p365 Fig.5.50|||Post-tectonic intrusion. Forms prominent, massive unfoliated outcrops. Early Permian?|||||Pale pink, medium-grained, porphyritic hornblende-biotite monzogranite.|
75627|Grant Creek Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, moderately porphyritic (hornblende-) biotite monzogranite; with scattered mafic inclusions up to c. 40 cm across and traces of titanite, allanite; locally with small, vuggy pegmatitic patches.|
80774|Grass Humpy Gabbro|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Gabbro.|
26267|Grass Hut Granite|22847|3|Fully described|p 43||Ordovician|Pb/Pb age 463 +/-3Ma||||||
26267|Grass Hut Granite|23422|5|Briefly described|p172, p209 Table 6.6|Ordovician|Ordovician|Of Lavery Creek Supersuite.||||||
26267|Grass Hut Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 108.||||||
26267|Grass Hut Granite|42245|2|Defined|p33|Ordovician||||||||
26267|Grass Hut Granite|43093|4|Described|Appendix 1|||Pb isotope age of 463+/-3Ma||||||
26267|Grass Hut Granite|43259|4|Described|Appendix 1,p23.||Ordovician|Ordovician?||||||
26267|Grass Hut Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
26267|Grass Hut Granite|62521|5|Briefly described|p6|Middle Ordovician|Middle Ordovician|Age: ~463+/-3Ma. Geological Province: Ravenswood Batholith.||||||14-JAN-08
26267|Grass Hut Granite|68731|6|Mentioned|p149|Middle Ordovician|Middle Ordovician||463 +/- 3 Ma, 207Pb/206Pb (Hutton et al. 1994a)|||||
26267|Grass Hut Granite|71592|5|Briefly described|Appendix A.|||Macrossan Igneous Province, Thomson Orogen.|463+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
35070|Grasstree Leucogranite|23049|3|Fully described|p47|Devonian|Silurian|Age: 398-409+/-12Ma. of Grasstree Suite.||||||
35070|Grasstree Leucogranite|23283|2|Defined|p23|Devonian|Silurian|||||||
35070|Grasstree Leucogranite|23499|5|Briefly described|map legend|Devonian|Silurian|Lolworth Batholith.||||||
35068|Grasstree Suite|23049|4|Described|p45|||||||||
35068|Grasstree Suite|23283|4|Described|p23|Devonian|Silurian|||||||
35068|Grasstree Suite|23422|4|Described|p177, p216 Table 6.10|||Probably Early Devonian.||||||
35068|Grasstree Suite|23430|5|Briefly described|p484-485|||Lolworth Batholith Province||||||
35068|Grasstree Suite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Broughton River, Amarra and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
35068|Grasstree Suite|69592|4|Described|p292|Early Devonian|Early Devonian|Northeast Lolworth Batholith, Charters Towers Province. High-K, calc-alkaline granites; geochemistry briefly described. This age determination may be of an Amarra Suite xenocryst.|414 +/- 5 Ma (SHRIMP U -Pb zircon).||Grasstree Granite.|Intrudes Cape River Metamorphics and the Amarra Suite.|Garnet-muscovite leucogranite, pegmatite and aplite; layered dykes and subhorizontally layered sheets. S-type.|
35068|Grasstree Suite|72528|5|Briefly described|p84.|Early Triassic|Lopingian||251.2+/-1.3 Ma U-Pb SHRIMP||Includes Malara Quartz Monzodiorite|Age from Malara Quartz Monzodiorite.||
27083|Graveyard Creek Group|23032|5|Briefly described|p21,24,53 fig6|||||||||
27083|Graveyard Creek Group|23044|6|Mentioned|59|||Broken River Province||||||
27083|Graveyard Creek Group|23423|5|Briefly described|p267||Silurian|Broken River Province.||||||
27083|Graveyard Creek Group|23424|5|Briefly described|Table 8.1 Fig 8.3 p333|Late Silurian|Early Silurian|Graveyard Creek Subprovince.||||||
27083|Graveyard Creek Group|23430|5|Briefly described|471p|||Underlying Unit Judea Formation. Broken River Province.||||||
27083|Graveyard Creek Group|23431|5|Briefly described|p542|||||||||
27083|Graveyard Creek Group|23619|5|Briefly described|p17||Llandoverian|||||||
27083|Graveyard Creek Group|23893|5|Briefly described|p9 Fig. 4|Early Devonian|Ordovician|||||||
27083|Graveyard Creek Group|24029|5|Briefly described|p111, p113 Fig.1|||Includes Magpie Creek Limestone Member, Quinton Formation, Crooked Creek Conglomerate Member, Jack Formation and Poley Cow Formation.||||||16-MAR-05
27083|Graveyard Creek Group|24613|5|Briefly described|p6 Fig. 3|Early Devonian|Ordovician|Geological province: Burdekin Basin.||||||07-FEB-11
27083|Graveyard Creek Group|41260|3|Fully described|p36|||Originally defined as Graveyard Creek Formation||||||
27083|Graveyard Creek Group|41719|1|Redefined|p215|Early Devonian|Early Silurian|||||||
27083|Graveyard Creek Group|41739|6|Mentioned|p306|||||||||
27083|Graveyard Creek Group|42031|5|Briefly described|p760|||||||||
27083|Graveyard Creek Group|42054|6|Mentioned|p273|||||||||
27083|Graveyard Creek Group|42279|6|Mentioned|p28|||||||||
27083|Graveyard Creek Group|42692|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27083|Graveyard Creek Group|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27083|Graveyard Creek Group|42709|6|Mentioned|map legend|||||||||
27083|Graveyard Creek Group|42752|4|Described|p47|||||||||
27083|Graveyard Creek Group|42933|3|Fully described|p55|||supersedes Graveyard Creek Formation||||||
27083|Graveyard Creek Group|43113|5|Briefly described|p32|||||||||
27083|Graveyard Creek Group|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
27083|Graveyard Creek Group|50096|5|Briefly described|p75|Early Devonian|Silurian|Includes the Jack Formation.||||||
27083|Graveyard Creek Group|60425|5|Briefly described|p115|Early Devonian|Silurian|Age is Late Llandovery-Lochkovian?  Part correlates with Chillagoe Formation.||||||07-FEB-11
27083|Graveyard Creek Group|61727|5|Briefly described|p942 Fig.1|Early Devonian|Silurian|Geological Province: Broken River Province/Graveyard Creek Subprovince. See also p952.||||||
27083|Graveyard Creek Group|61894|5|Briefly described|p182|Late Silurian|Late Silurian|Broken River area.|||Jack Formation.|||
27083|Graveyard Creek Group|63154|5|Briefly described|p281 Fig. 3|Silurian|Silurian|Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
27083|Graveyard Creek Group|67848|5|Briefly described|p3 Fig.2, p14, p16.|Late Silurian|Late Silurian|Part of forearc basin component of the arc-trench gap succession involved in collisional accretion. Promoted to Graveyard River Group in Fig.2.|||Includes Crooked Creek Conglomerate.|||
27083|Graveyard Creek Group|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.|||Includes Crooked Creek Conglomerate; Quinton, Poley Cow and Jack Formations.|||
27083|Graveyard Creek Group|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.|||Includes Crooked Creek Conglomerate; Quinton, Poley Cow and Jack Formations.|||
27083|Graveyard Creek Group|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince. Contains evidence of NW-SE shortening.|||Includes Jack Formation and Poley Cow Formation.|||
27083|Graveyard Creek Group|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince. Contains evidence of NW-SE shortening.|||Includes Jack Formation and Poley Cow Formation.|||
27083|Graveyard Creek Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Broken River Province.||||||
27083|Graveyard Creek Group|69030|5|Briefly described|p6, p17|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province). Hosts significant gold mineralisation.|||Crooked Creek Conglomerate; Quinton, Poley Cow, Jack Formations; Magpie Creek Limestone.||Marine shelf clastic rocks and limestone.|
27083|Graveyard Creek Group|69079|6|Mentioned|p5, p63, p68|Early Devonian|Early Silurian|Graveyard Creek Subprovince, Broken River Province. Hosts sporadically-distributed gold-antimony mineralisation in fissure veins (described in some detail).||||||
27083|Graveyard Creek Group|69592|4|Described|p251 Fig.4.35, p254-255, p258-268|Devonian|Late Silurian|See also p272 Fig.4.61, p274 Fig.4.65, p277, p296-298, p303. Graveyard Creek Subprovince, Broken River Province. Carbonate-rich. Thickness ranges from >5,000m to 150m. Deformation described.|||Crooked Creek Conglomerate; Poley Cow, Jack, Shield Creek Formations.|Overlies Netherwood Tonalite nonconformably and Judea Formation unconformably. Is overlain by Broken River Group.|Coralline and stromatoporoid limestone; intervals with deeper marine siliciclastic rocks including conglomerate and distinctive calcirudite horizons.|
27083|Graveyard Creek Group|73201|6|Mentioned|p609, p610|Devonian|Silurian|Broken River Province, Graveyard Creek Subprovince. Predominantly shallow marine strata. Setting interpreted as a forearc basin.||||||
37901|Greasy Creek granodiorite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
79608|Green Creek Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier.|1738 +/- 3 Ma.|||||
79608|Green Creek Granite|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian|Shown in Mary Kathleen Domain column. A-type granitoid.?Of Burstall Suite. p3 suggests these granites intrude the Mary Kathleen Domain.|1738 +/- 3 Ma SHRIMP zircon.|||||16-JAN-17
79608|Green Creek Granite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Kalkadoon-Leichhardt Domain.|||||Felsic intrusive.|
29745|Green Rock Quartz Monzonite|22845|6|Mentioned|Fig6|Triassic|Triassic|||||||
29745|Green Rock Quartz Monzonite|22846|2|Defined|p55,6|Triassic|Carboniferous|Central section of the Station Creek Batholith.||||||
29745|Green Rock Quartz Monzonite|23608|5|Briefly described|p49-51|||Now incorporated in Woolooga Granodiorite and the 'Gibraltar Quartz Monzodiorite'.||||||
29745|Green Rock Quartz Monzonite|23609|5|Briefly described|p11|||Replaced by Green Rock Quartz Monzodiorite to reflect the rock type. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
29745|Green Rock Quartz Monzonite|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
29745|Green Rock Quartz Monzonite|68679|5|Briefly described|p411|Late Triassic|Late Triassic|Southern part of the northern New England Orogen. Wedge-shaped outcrop area ~20 km2, between Station Creek Quartz Monzonite and Mount Mucki Complex.||Station Creek Igneous Complex.||Gradational boundary with Green Rock Quartz Monzonite.|Biotite-quartz-hornblende monzonite.|
28256|Greenbank Quartz Diorite|24382|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|||||||
28256|Greenbank Quartz Diorite|41778|2|Defined|Table 1|Middle Triassic|Early Triassic|Described P373. Reserved as Greenbank.||||||14-AUG-08
28256|Greenbank Quartz Diorite|43008|5|Briefly described|map legend|||||||||
28256|Greenbank Quartz Diorite|63821|4|Described|p30|Middle Triassic|Early Triassic|Intrudes Nour Nour Granodiorite and sediments of the Curtis Island Group. Comprises medium- to coarse-grained biotite-hornblende quartz diorite on the eastern margin and fine- to medium-grained biotite quartz diorite in the central part of the pluton.||||||07-FEB-11
28256|Greenbank Quartz Diorite|64399|5|Briefly described|Map legend|Triassic|Triassic|Biotite-hornblende quartz diorite, biotite pyroxene quartz diorite.||||||
28256|Greenbank Quartz Diorite|68679|5|Briefly described|p421-422|||Gayndah-Gladstone belt.|||||Fine- to medium-grained, biotite-hornblende quartz diorite, biotite-pyroxene quartz diorite; altered on the eastern margin; fresher biotite quartz diorite in central areas.|
77822|Greencoat Quartz Monzonite|65388|2|Defined|p347-348, p46, p305, 306, 340|Late Triassic|Late Triassic|Previously NW part of the Mount Saul Adamellite. Intrudes Narayen beds. inferred to intrude Carboniferous Evandale Tonalite. Age uncertain. Inferred from similar Mount Saul Quartz Monzonite. Pinkish grey, medium to coarse-grained, equigranular to slightly porphyritic quartz monzonite.||||||
77822|Greencoat Quartz Monzonite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
77822|Greencoat Quartz Monzonite|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|This unit, as well as the Boolgal Granophyre and Mount Saul Quartz Monzonite, are all mapped under the symbol, Rgr.||||||30-SEP-15
77822|Greencoat Quartz Monzonite|68679|5|Briefly described|p312, p428-429, p441|Late Triassic|Late Triassic|Withnall et al. (2009). Northern New England Orogen. Forms stocks. Is associated with the Morang Volcanics and Mount Saul Quartz Monzonite.|||||Medium- to coarse-grained, equigranular to slightly porphyritic hornblende-biotite quartz monzonite with a small area of medium-grained leucocratic biotite monzogranite in the northeast.|
36616|Greenes Spring granodiorite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36616|Greenes Spring granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 417.  I-Type.||||||
83084|Greens Creek Quartz Monzonite|73553|5|Briefly described|p18, p32-33, p35-36, p73-75,|Statherian|Statherian|Mary Kathleen Domain. Wonga Igneous Subprovince. Previously included in Wonga Granite by Carter (1959) and Derrick et al., (1977a), described by Pearson et al., (1992, p.294) as unnamed subunit '3a' of the Wonga Granite. Mainly mottled white and pale blue tones on radiometric images, displays very low responses on aeromagnetic images. Mainly in contact with Argylla Formation, post-dates Rosebud Granite and probably pre-dates Natalie Granite. Cut by metadolerite and schistose amphibolite dykes. Mostly A-type. See also p78-81, p83, p100-101, p118, p246-247, p249.|1738+/-3 Ma U-Pb zircon SHRIMP||||Strongly foliated to gneissic and locally mylonitic, extensively recrystallised, fine-to medium-grained, porphyritic amphibole-biotite quartz monzonite.|03-FEB-23
39067|Grevillea Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
39067|Grevillea Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province. The 2 facies are mapped separately.|||||White to light grey, coarse-grained equigranular to porphyritic granite; white, very fine to fine-grained leucogranite.|
39067|Grevillea Granite|68679|5|Briefly described|p428, p431-432|Late Triassic|Late Triassic|Northern New England Orogen. Forms steep, rugged terrain in the Grevillea Range.|||||White to light grey, coarse-grained, equigranular to porphyritic granite with sodic amphibole; A-type alkali feldspar granite; not peralkaline; white, fine-grained leucogranite phase.|
39067|Grevillea Granite|73450|4|Described|p9, p15-19, p21, p35|late Triassic|late Triassic|A-type. Previously mapped partly as Curtis Island Group and partly as Miriam Vale Granodiorite (Ellis, 1974). Forms a roughly ovoid, northerly aligned pluton SSW of Lowmead; forms the Grevillea Range. Not yet radioisotopically dated although it is most probably late Triassic.|||||Very pale pink to pale pink or buff to pale brown, medium- to fine-grained, uneven-grained to slightly porphyritic, leucocratic alkali feldspar granite with sparse enclaves of pale to dark brown microgranite and diorite.|
23638|Greybank Volcanics|22800|5|Briefly described|Fig.14 p592|Famennian|Famennian|See also p591, p592||||||
23638|Greybank Volcanics|23161|6|Mentioned|p12||Late Devonian|||||||
23638|Greybank Volcanics|23522|5|Briefly described|p250 Fig 6|Late Devonian|Late Devonian|||||||
23638|Greybank Volcanics|42747|5|Briefly described|p39, Fig.2|||see also Fig.10||||||
23638|Greybank Volcanics|43029|5|Briefly described|Fig.1,p13|||||||||
23638|Greybank Volcanics|43204|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Anakie Inlier||||||23-DEC-11
23638|Greybank Volcanics|43213|2|Defined|p9,p67,p69-75, p93, p117, p121-129, p190|Frasnian|Frasnian|See also p227. New (modified) name in this Report: formerly 'Greybank Andesite' (Plibersek and Browne, 1986), for a sequence near Greybank Bore which had been mapped as Theresa Creek Volcanics by Olgers (1969). Generalised composite type section detailed. Fletchers Awl dome. Age from brachiopods and conodonts discussed. Possibly the oldest rocks in the Drummond Basin sequence in this study area. Lithologies described in some detail. Correlative of Dee Volcanics and Boulder Creek Grit. Hosted subeconomic Au and Cu mineralisation. Chemical analyses detailed.||||Unconformably overlies Mooramin Granite. Is intruded by dykes of Peak Range Volcanics. Is overlain by Silver Hills Volcanics conformably, and Back Creek Group unconformably.|Basal quartzose sandstone, siltstone and conglomerate; overlain by undivided intermediate volcanic breccias, lava flows, volcaniclastic sediments and pyroclastics; locally subdivided.|
23638|Greybank Volcanics|60705|5|Briefly described|p658|Famennian|Frasnian|Andesitic volcanics. Geological Province: Drummond Basin||||||12-APR-05
23638|Greybank Volcanics|65214|6|Mentioned|p282|Devonian|Devonian|QLD, Ukalunda. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23638|Greybank Volcanics|66084|5|Briefly described|Map legend|Carboniferous|Late Devonian|Aphyric to porphyritic andesite to dacite lava and minor volcaniclastic breccia, siltstone and mudstone; minor quartzose sandstone and limestone. In upper part, locally pebble to boulder polymictic conglomerate and feldspatholithic arenite.   ||||||
23638|Greybank Volcanics|68553|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|||||||
23638|Greybank Volcanics|68731|5|Briefly described|p130, p131, p177 Fig 3.91, p193|Late Devonian|Late Devonian|Plibersek and Browne (1986); Blake, Withnall and Hayward (1995). Drummond Basin/Ukalunda Shelf. ~ 2400 m thick. Conodonts from this unit indicate late and latest crepida Zone of the early Famennian (Mawson and Talent 2003).||||Nonconformably underlain by the Mooramin Granite.|Comprises volcaniclastic conglomerate, sandstone, siltstone, and andesite.|10-MAY-16
23638|Greybank Volcanics|68900|6|Mentioned|p4, p49|Early Carboniferous|Late Devonian|Drummond Basin.||||||
23638|Greybank Volcanics|73179|6|Mentioned|p1143|Late Devonian|Middle Devonian|Anakie Inlier.|||||Predominantly basaltic to andesitic.|
73901|Greymare Suite|63748|6|Mentioned|p28|Early Triassic|Permian|Includes the Greymare Granite.||||||07-FEB-11
73901|Greymare Suite|68679|5|Briefly described|p457, p464|Permian|Permian|Northern New England Batholith.|~280 Ma.|Clarence River Supersuite.|Greymare Granodiorite.|||
73901|Greymare Suite|71628|5|Briefly described|p18: 10|||||Greymare Supersuite.|Greymare Tonalite.|||
73900|Greymare Supersuite|63748|6|Mentioned|p28|Early Triassic|Permian|Includes the Greymare Suite.||||||07-FEB-11
73900|Greymare Supersuite|71628|5|Briefly described|p18: 1, 10||||||Greymare Suite.||I-type.|
82756|Greymare Tonalite|71628|4|Described|p18: 1-2, 10-13, 16; p19:5|||Butler (1974). Originally the Greymare Granite (Richards, 1918); subsequently Greymare Granodiorite (Robertson, 1970). Name derived from the locality of the same name. Forms an ovoid intrusion ~11 x 6 km, about 30 km W of Warwick. Crops out, generally poorly, as scattered boulders. Lithology, mineralogy and geochemistry described in some detail.|279.6 +/- 2.6 Ma (SHRIMP: Donchak et al., 2007).|Greymare Suite.||Intrudes Texas beds.|Grey, speckled, fine- to medium-grained, mildly porphyritic to uneven-grained, quartz-rich biotite(-hornblende) tonalite to granodiorite; slightly to moderately deformed. Is cut by dykes. I-type.|
78929|Greystone Granodiorite|65388|3|Fully described|p316-318, p295, 303, 304, 331, 339-340|Early Triassic|Early Permian|Of Coonambula Suite. Replaces Greystone Granite. Names used interchangeably p295 for same six samples with  geochemical affinities to early Permian Coonambula Suite rocks. 3 other samples show similarities to Tandora Suite.  Further work is needed to resolve the distribution of these different suites within the Greystone Granodiorite as currently mapped. Outcrop poor. Intrusive relationships with adjacent granites are not known.  Includes gneissic rocks and biotite granite.||||||
78929|Greystone Granodiorite|68679|5|Briefly described|p419|||Rawbelle Batholith. ~200 km2. Geochemistry suggests unit is composite; six analyses plot within Coonambula Suite while three others plot within Tandora Suite.||||Is overlain by Mount Eagle Volcanics.|Biotite granodiorite and (hornblende-)biotite granodiorite. Gneissic rocks mapped in unit probably Coonambula Granodiorite. Mafic rocks in the west similar to Glencoe Gabbro suggest complex intermixing.|
26596|Gudman Oolite|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Crg].  Pisolitic and oolitic limestone, fossil-bearing sandstone, minor siltstone.||||||
26596|Gudman Oolite|31519|6|Mentioned|p917|||||||||
26596|Gudman Oolite|31586|6|Mentioned|p6|||Correlation||||||
26596|Gudman Oolite|31657|5|Briefly described|p94|||U.Tournaisian to U.Visean||||||
26596|Gudman Oolite|31659|5|Briefly described|p52||Tournaisian|Basal unit of the Rockhampton Group, but not always recognisable outside the type area. Comprises pisolitic limestone at base and bioclastic limestone, separated by calcareous lithic sandstone.||||||09-JUN-09
26596|Gudman Oolite|32866|6|Mentioned|p9|||Fossil content||||||
26596|Gudman Oolite|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
26596|Gudman Oolite|34155|6|Mentioned|p91|||See P93. Tournaisian.||||||
26596|Gudman Oolite|38215|6|Mentioned|p276|||||||||
26596|Gudman Oolite|38406|6|Mentioned|p11|||||||||
26596|Gudman Oolite|39445|5|Briefly described|Table 6|||||||||
26596|Gudman Oolite|39973|6|Mentioned|p4|||||||||
26596|Gudman Oolite|41576|4|Described|Table 1|||||||||
26596|Gudman Oolite|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
26596|Gudman Oolite|41826|6|Mentioned|p325|||||||||
26596|Gudman Oolite|41925|6|Mentioned|p45|||||||||
26596|Gudman Oolite|42547|4|Described|p49|||||||||
26596|Gudman Oolite|42583|5|Briefly described|p66|||||||||
26596|Gudman Oolite|44360|14|Not recorded|p2,30,31||Tournaisian|Northern equivalent of Herring Gully Limestone Member||||||
26596|Gudman Oolite|44379|14|Not recorded|p15|||Ref. to Fleming 1967.||||||
26596|Gudman Oolite|44388|2|Defined|p113-116||Tournaisian|Conformably overlain by Malchi Formation. (Late Tournaisian)||||||
26596|Gudman Oolite|45097|6|Mentioned|Fig.|||Correlation chart||||||
26596|Gudman Oolite|46803|6|Mentioned|p143|||See also Fig. 4||||||
26596|Gudman Oolite|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Rockhampton Group.||||||17-MAY-04
26596|Gudman Oolite|61557|6|Mentioned|p878.|||Of Fleming (1967). Obsolete name for the Gudman Formation.||||||
26596|Gudman Oolite|68008|4|Described|p90,p93, p95-96, p104-105,p107,p582,p594|Early Carboniferous|Early Carboniferous|Fleming (1967). Not reliably recognised outside the Stanwell area. Detailed facies description.||Rockhampton Group.||(An equivalent) is overlain by Malchi Formation (equivalent). Correlated with the Herring Gully Limestone Member.|Oolitic/pisolitic limestone with relatively large intervals of sandstone or siltstone.|
26596|Gudman Oolite|68679|5|Briefly described|p340|||Fleming (1967).||Rockhampton Group.||Correlated with the Herring Gully Limestone Member.||
28164|Guela Sandstone|23291|4|Described|p83 Tb. 3.6|Early Paleozoic|Mesoproterozoic|Parent: Inorunie Group. Thickness: 300m? Geological Province: Georgetown Region.||||||30-JUN-15
28164|Guela Sandstone|40218|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
28164|Guela Sandstone|40954|6|Mentioned|p132|||||||||
28164|Guela Sandstone|41975|6|Mentioned|Fig.3 P433|||||||||
28164|Guela Sandstone|43664|6|Mentioned|Fig.3,p15|||||||||
28164|Guela Sandstone|68355|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Chulcee Formation. Is overlain conformably by Arrongulla Formation.|White to pale pink or yellow-brown, thick-bedded, fine- to coarse-grained orthoquartzite; micaceous quartzose sandstone.|
28164|Guela Sandstone|68356|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin.||Unit in Inorunie Group.||Conformably overlies Chulcee Formation. Is overlain conformably by Arrongulla Formation.|White to pale pink or yellow-brown, thick-bedded, fine- to coarse-grained orthoquartzite; micaceous quartzose sandstone.|
28164|Guela Sandstone|69591|5|Briefly described|p75|||Croydon Province, Georgetown Inlier.||Inorunie Group.||||
78315|Guide Supersequence|63866|5|Briefly described|p53, p56, p58|Statherian|Statherian|Leichhardt Superbasin.|c. 1800-1780 Ma||Includes the Mount Guide Quartzite.|(Possibly) equivalent to the Yiyintyi Sandstone and the Westmoreland Conglomerate. Overlain by the Eastern Creek Volcanics.||
78315|Guide Supersequence|65505|6|Mentioned|979|Proterozoic|Proterozoic|Of the Leichhardt River Fault Trough. Age: 1800-1785 Ma.||||||
78315|Guide Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p9|||Of Jackson and others (2000). Shown as an alternate name for Mount Guide Quartzite. Leichhardt Superbasin.|~1800-1775 Ma.|||Is overlain by Myally Supersequence.||
78315|Guide Supersequence|68021|5|Briefly described|p134 Fig 3, p135, 136|Statherian|Statherian|Leichhardt Superbasin. Fluviatile to lacustrine sedimentary packages intruded by dolerite dykes.|1800-~1785 Ma||Includes Mount Guide Quartzite and Bottletree Formation.|||
78315|Guide Supersequence|68732|5|Briefly described|p159, p161, p167, p170-171|||Typically relatively shallow-water shelf facies deposits.|||Includes Mount Guide Quartzite and Bottletree Formation.|||30-NOV-17
78315|Guide Supersequence|69591|5|Briefly described|p27, p32-33|||Leichhardt River Domain, Leichhardt Superbasin, Mount Isa Province. Deposition in N-trending rifts or half-grabens comprises the syn-rift Bottletree Formation and lower Mount Guide Quartzite, succeeded by finer-grained, post-rift upper Mount Guide Quartzite.|||||An early (syn-rift) phase of felsic volcanism was followed by deposition of fluvial to shallow marine (post-rift sag phase) clastic successions.|
78315|Guide Supersequence|72912|5|Briefly described|p12.|Paleoproterozic|Paleoproterozic|Leichhardt Superbasin, Mount Isa Province.|||Bottletree Formation, Mount Guide Quartzite, Eastern Creek Volcanics, the Magna Lynn Volcanics, Argylla Formation.||Includes felsic and mafic volcanic rock, flood basalts and fluvial to shallow marine quartzites.|
28254|Gumbardo Formation|22464|6|Mentioned|p9||Early Devonian|Adavale Basin. Overlain by Eastwood Beds||||||
28254|Gumbardo Formation|22518|6|Mentioned|p 10|||||||||
28254|Gumbardo Formation|22604|6|Mentioned|p442|||||||||
28254|Gumbardo Formation|22857|6|Mentioned|p201|||Andesite. Geological Province: Avadale Basin. ||||||
28254|Gumbardo Formation|22859|6|Mentioned|p201|||||||||
28254|Gumbardo Formation|23522|5|Briefly described|p250 Fig 6|Emsian||||||||
28254|Gumbardo Formation|23834|4|Described|p312|Emsian|Emsian| Geological Province: Adavale Basin. Maximum thickness: >43m.||||||
28254|Gumbardo Formation|29387|6|Mentioned|Table 1|||Refers to Galloway(1970). Lower Devonian.||||||
28254|Gumbardo Formation|29393|6|Mentioned|Table 1|||Lower Devonian.||||||
28254|Gumbardo Formation|29721|6|Mentioned|Table 38|||||||||
28254|Gumbardo Formation|30103|4|Described|p5|||Table 2 on p5. See also p6.||||||20-NOV-08
28254|Gumbardo Formation|30104|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|30544|6|Mentioned|Fig.5 P51|||Devonian||||||
28254|Gumbardo Formation|30691|4|Described|p7|||See also Table 6. Middle Devonian age||||||
28254|Gumbardo Formation|30853|1|Redefined|p27|Middle Devonian|Middle Devonian|See also Table 2.||||||
28254|Gumbardo Formation|30854|4|Described|Table 2|||Middle Devonian age||||||
28254|Gumbardo Formation|30855|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|31999|5|Briefly described|Table 1|||||||||
28254|Gumbardo Formation|32619|6|Mentioned|p462|||L.Dev.||||||
28254|Gumbardo Formation|33069|4|Described|p6|||Middle Devonian.||||||22-DEC-09
28254|Gumbardo Formation|33078|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|33079|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|33087|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||22-DEC-09
28254|Gumbardo Formation|33088|4|Described|Table 2|||Of the Adavale Group.||||||20-NOV-08
28254|Gumbardo Formation|33092|5|Briefly described|p5|||Stratigraphy||||||
28254|Gumbardo Formation|33326|6|Mentioned|p447|||Fauna.||||||
28254|Gumbardo Formation|33641|6|Mentioned|p59|||L.Dev.||||||
28254|Gumbardo Formation|33732|6|Mentioned|p103|||Emsian.||||||
28254|Gumbardo Formation|34065|4|Described|p7|||Middle Devonian.||||||20-NOV-08
28254|Gumbardo Formation|34217|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
28254|Gumbardo Formation|34218|4|Described|Table 1|||See also Table 2, p8. Middle Devonian.||||||20-NOV-08
28254|Gumbardo Formation|37565|6|Mentioned|Fig.6|||||||||
28254|Gumbardo Formation|38226|6|Mentioned|p414|||||||||
28254|Gumbardo Formation|39445|5|Briefly described|Table 5|||See also p73.||||||20-NOV-08
28254|Gumbardo Formation|39478|6|Mentioned|Table 1|||||||||
28254|Gumbardo Formation|39480|6|Mentioned|p188|||||||||
28254|Gumbardo Formation|40762|6|Mentioned|p282|||||||||
28254|Gumbardo Formation|40787|6|Mentioned|p340|||||||||
28254|Gumbardo Formation|41097|6|Mentioned|Table 1|||||||||
28254|Gumbardo Formation|41167|6|Mentioned|p398|||||||||
28254|Gumbardo Formation|41198|5|Briefly described|p35|||Mention Table 1||||||
28254|Gumbardo Formation|41208|6|Mentioned|Fig.1|||||||||
28254|Gumbardo Formation|41289|6|Mentioned|p209|||||||||
28254|Gumbardo Formation|42031|5|Briefly described|Fig.8 P766|||||||||
28254|Gumbardo Formation|42999|5|Briefly described|p87,Table1.p90|||||||||
28254|Gumbardo Formation|43004|5|Briefly described|Table 1,p179|||||||||
28254|Gumbardo Formation|43008|5|Briefly described|map legend|||||||||
28254|Gumbardo Formation|43105|5|Briefly described|p11|||||||||
28254|Gumbardo Formation|43213|5|Briefly described|p93|Emsian|Emsian|Adavale Basin.||||Is overlain by Eastwood beds.|Continental felsic to mafic volcanics.|
28254|Gumbardo Formation|43461|14|Not recorded|p617,table p618||Early Devonian|||||||
28254|Gumbardo Formation|43914|14|Not recorded|p3,Fig.3|||K-Ar: 380 Ma.||||||
28254|Gumbardo Formation|44770|14|Not recorded|p111,diag.p113,114|||Part of Adavale Group.||||||
28254|Gumbardo Formation|44851|14|Not recorded|p172||Middle Devonian|Part of Adavale Group.||||||
28254|Gumbardo Formation|44888|14|Not recorded|p32|||||||||
28254|Gumbardo Formation|44889|14|Not recorded|p160||Silurian|K/Ar = Middle Devonian||||||
28254|Gumbardo Formation|46881|6|Mentioned|Table.1|||See also Table.2||||||
28254|Gumbardo Formation|48920|6|Mentioned|Fig.2|||See also Table 3||||||
28254|Gumbardo Formation|64783|1|Redefined|p88-91, p82, p84-87,92-94, 100, 103, 104|Emsian|Pragian|First named by Phillips Petroleum Company (1963) in PPC Gumbardo-1, and defined by them in 1964; the reference section being 3167.8 to 3912.1 m.  Redefined here as the section between 3148.5 and 3904 m, to exclude Ordovician volcanic rocks. Galloway (1970) included in the Formation the eastern-margin arkosic and labile arenites. Basal unit in Adavale Basin. Pragian to early-mid Emsian.|408.3 +/- 2.4 Ma and 401-8 +/- 2.1 Ma.|||Is unconformably overlain by Eastwood beds, Log Creek Formation or Etonvale Formation.|Includes volcanic and volcaniclastic rocks including arkosic and litho-feldspathic labile sandstones, and acidic volcanics (crystal tuffs and ignimbrite) with minor mafics.|15-NOV-17
28254|Gumbardo Formation|65214|6|Mentioned|p275|Devonian|Devonian|QLD, Adavale. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
28254|Gumbardo Formation|65756|5|Briefly described|p27|Early Devonian|Early Devonian|||||||
28254|Gumbardo Formation|67402|5|Briefly described|p165 tbl LPB1, p167|Emsian|Pragian|Adavale Basin. Deposited as fluvio-lacustrine rift infill continental sediments. See also p168 tbl ADV/WRR1, p170, fig ADV/WRR8, p172, p173, p175.||||Overlain by the Eastwood beds.|Andesitic basalt, rhyolite, trachyandesite and volcaniclastic arkosic and litho-feldspathic labile sandstones becoming more silty/muddy towards the northeast of the basin.|
28254|Gumbardo Formation|68731|5|Briefly described|p164, p174, p179, pp180-181 Tb 3.3|Early Devonian|Early Devonian|Adavale Basin. Evans et al. (1990), de Boer (1996), and Boreham and De Boer, (1998). Between 25.6-755.5 m thick. Suggested fluvial and perhaps fluvio-lacustrine depositional environment.|402 +/- 2 Ma; 408 +/- 4 Ma (McKillop et al. 2007)|||Unconformably overlain by the Log Creek Formation.|Comprises volcanic and volcaniclastic rocks. Volcaniclastics are feldspathic and lithofeldspathic labile sandstones. Volcanic rocks are mainly acidic, although there are some mafic volcanic rocks.|
28254|Gumbardo Formation|69541|5|Briefly described|p645 Fig.1(b), p654|Emsian|Pragian|Thomson Orogen. Oldest unit in the Adavale Basin. Subsurface.||||Is overlain by Eastwood beds.|Volcanic and volcaniclastic rocks.|
28254|Gumbardo Formation|70744|5|Briefly described|p939|Early Devonian|Early Devonian|Thomson Orogen basement (QLD).|c.409 Ma (estimated from Fig.7).|||||
28254|Gumbardo Formation|70823|5|Briefly described|p33|Devonian|Silurian|Cooper Basin.||||||
28254|Gumbardo Formation|71965|6|Mentioned|p913-914|Devonian|Devonian|Of Adavale Basin.||||||
28254|Gumbardo Formation|71966|5|Briefly described|p989,991,997,1000,1002|Early Devonian|Early Devonian|Of Adavale Basin. Volcanism associated with the opening of the Adavale Basin as a result of 408-403 Ma extension. Intersected in drillholes PPC Carlow 1 and PPC Gumbardo 1, and sample of rhyolitic ignimbrite analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 1682891 yielded a 206Pb/238U age of 408.1+\-3.1 Ma, interpreted as the eruptive age of ths sample. Sample 1682892 yielded a weighted mean 206Pb/238U age of 402.9+\-2.9 Ma, interpreted as crystallisation age of the rock. SHRIMP U-Pb ages constrain the lower age and initial phases of basin opening to approximately Pragian (Draper 2006). Contains c. 475 ma inherited zircons, derived from local volcanic or plutonic source that was mixed into the ignimbirite during eruption or later phase of magmatic evolution. Hf and O isotope analysis indication derivation from a more juvelie source than Silurian granites.|||||Volcanic and volcaniclastic rocks including rhyolitic ignimbrite.|25-OCT-19
28254|Gumbardo Formation|72522|6|Mentioned|p1.|Early Devonian|Early Devonian|Located in the Adavale Basin c. 200km north of the central Thomson Orogen. Age of ignimbrites in this unit stated to be indistinguishable from Maximum depositional age of volcaniclastic sandstone in Paka Tank Trough (398+/-3 Ma).|||||Includes ignimbrites.|
28254|Gumbardo Formation|73179|4|Described|p1133, p1136-1143, p1147-1156|Emsian|Pragian|Adavale Basin. Deposited in a half-graben system that appears to be confined to a NNE-SSW-trending rift corridor. Found in the main depocentre of the basin and may extend [at depth] to the Warrabin and Quilpie troughs based on seismic interpretations. Used as a seismic marker horizon.  Maximum thickness: 755.5 m. Geochron are previously published SHRIMP ages, which are reportedly slightly older than new LA-ICP-MS ages.  [Article includes detailed thin section petrography, a series of new U-Pb LA-ICP-MS ages and whole-rock geochemistry]. Epiclastic sedimentary rocks both underlie and overlie volcanic units. Ignimbrites are interpreted as an outflow facies [relatively distal from source]. Similar ages for ignimbrites suggest short-lived volcanism at the initiation of the basin opening. Has inherited zircons but lacks inherited ages between 600 and 500 Ma, which is a prominent detrital zircon age in metasedimentary rocks of the Thomson Orogen; [thus,] little to no contribution of metasedimentary rocks in the petrogenesis of this unit. Volcanics have transitional I- to A-type affinities.|402.9 +/- 2.9 Ma, 408.1 +/- 3.1 Ma|||Unconformably overlain by Eastwood Beds.|Dominantly crystal-rich dacitic and rhyolitic ignimbrites with porphyritic rhyolite and rhyodacite, tuff, very fine- to coarse-grained sandstone, pelitic sandstone and epiclastic sandstone (lithic arkose - arkose). [+/- andesite and andesitic tuff].|19-SEP-22
28254|Gumbardo Formation|73307|5|Briefly described|p585|||Basal unit in Adavale Basin.|c.410 Ma (Draper, 2006).||||Fluvial sedimentation followed by a marine incursion resulting in mixed carbonate-siliciclastic deposition.|
28015|Gumhole Monzogranite|23420|5|Briefly described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Yellowood Granodiorite.||||||
28015|Gumhole Monzogranite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Sugarbag Creek Quartzite and Astrea Formation. Medium to dark grey equigranular to slightly porphyritic biotite monzogranite.||||||15-JAN-09
28015|Gumhole Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
81236|Gun 1|66844|3|Fully described|p243, p254, p255-264, 266, 272, 273.|||Upper Gunpowder Creek-Paradise Creek Depositional Sequence (Gun 1.1-1.8). Details of fourth order sequences in Table 2 p258-263. Lawn Hill Platform. Marks the transition from siliciclastic to carbonate ramp; storm-dominated shallow water carbonates that progrades eastward over underlying siliclastics. Broad, regionally extensive facies belts and minor thickness variations due to uniform accommodation rates. Characterised by 7 stacked shallowing upwards sequences (see p251-254 for detailed lithofacies descriptions).  Subdivided into 8 fourth-order sequences (Gun 1.1-1.8); refer to p247-250, 255-263 for detailed illustrations and further definitions and criteria. See p265-267 for sequence stratigraphic analysis.||Of Gun Supersequence.|Gun 1.1 to Gun 1.8 fourth order sequences.|||
81237|Gun 2|66844|3|Fully described|p243, 247-250, 254-264, 267, 272, 273|||Upper Paradise Creek-Esperanza Depositional Sequence (Gun 2.1-2.5).  Details of fourth order sequences in Table 2 p258, 261. Lawn Hill Platform. Storm-dominated carbonate/siliciclastic ramp. Characterised by spar-rich microdigitate and digitate columnar stromatolites. Regionally extensive facies belts with localised sediment influx leading to local thickness variations. Characterised by 6 stacked upward-shallowing lithofacies (see p254-264 for detailed lithofacies descriptions). refer to p247-250, 255-263 for detailed illustrations and further definitions and criteria. See p267-269 for sequence stratigraphic analysis.||Of Gun Supersequence.|Gun 2.1 to Gun 2.5 fourth order sequences.|||
40575|Gun Supersequence|62535|5|Briefly described|p663, p672-674|||Isa Superbasin. Closely comparable to age of middle Paragon Group. Deposition followed a 15-20 m.y. hiatus.|c.1670 Ma - c.1650 Ma.|||Unconformably overlies Prize Supersequence.|Thick suite of stromatolitic carbonates (Lawn Hill Platform), and rhythmically laminated siliciclastic rocks (Leichhardt River Fault Trough).|
40575|Gun Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Masterton Sandstone and lower parts of Mallapunyah Formation.|||
40575|Gun Supersequence|63114|5|Briefly described|p1253 Fig.2, p1270,|||Isa superbasin.|||Includes the Esperanza, Paradise Creek, Gunpowder Creek Formations; Torpedo and Warrina Park Quartzites; Native Bee, Moondarra Siltstones; Breakaway, Urquhart Shales.|||
40575|Gun Supersequence|63866|4|Described|p53-p54, p57-p59, p61|Statherian||Isa Superbasin. Also includes the Native Bee Siltstone, Urquhart Shale, Spear Siltstone, Kennedy Siltstone and the Magazine Shale. Correlated with a unit of thick polymictic conglomerate in the Deighton Quartzite.|c. >1660 Ma||Includes the Masterton, Mallapunyah, Gunpowder Creek, Paradise Creek Formations, Moondarra Siltstone, Esperanaza Formation and the Paradise Creek Formation.|Conformably overlain by the Loretta Supersequence.||
40575|Gun Supersequence|65228|5|Briefly described|p16, pp23-26, Figs.11-14.|||First defined by Southgate et al (1999). Named after the Gunpowder Creek Formation which contains the maximum flooding surface. Constitutes basal McNamara Group in southern Lawn Hill Platform. Gamma ray log, lithology and facies detailed.||||||
40575|Gun Supersequence|65337|6|Mentioned|p32.|||This study includes all of the Drummond Formation as equivalents to this Supersequence.||||Overlies Prize Supersequence. Is overlain by Loretta Supersequence.||
40575|Gun Supersequence|65387|6|Mentioned|p1|||Western Fold Belt, Mt Isa Inlier. Possibly correlated with a psammite host of the Dugald River Pb-Zn deposit, aged 1686 +/- 7 Ma (detrital zircons).||||||
40575|Gun Supersequence|65396|6|Mentioned|p197|||Comprises most of the Mount Isa Group and western equivalents.||||||
40575|Gun Supersequence|66844|4|Described|p243-245,254, 265, 267, 270|||Lawn Hill Platform. Regionally extensive, southeast-facing, storm-dominated mixed carbonate/siliciclastic ramp. Separated from the underlying Prize SS by a regionally correlative unconformity in the lower to middle Gunpowder Creek Formation.||Equivalent to parts of lower McNamara Group.|Subdivided into Gun 1 and Gun 2 third-order depositional sequences, p254, 255-263.|Overlain by Loretta Supersequence (p255). Underlain unconformably by Prize Supersequence, and locally by Myally Sub Group||
40575|Gun Supersequence|67323|4|Described|GIS attrib tbl, p15, p39|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Isa Superbasin.|~1665-1655 Ma.|Mount Isa Group. ?McNamara Group||Overlies Prize Supersequence. Is overlain by Loretta Supersequence. Correlated with upper part of Deighton Quartzite.|Green and red siltstone, shale, micaceous siltstone, sandstone, laminated and stromatolitic dolomite, dolomitic siltstone, grey to white stromolitic chert, chert, and tuff|
40575|Gun Supersequence|68021|5|Briefly described|p135 Fig 4, p136|Statherian|Statherian|Equivalent to McNamara Group, Mount Isa Group, Marimo Slate in part, Soldiers Cap Group in part. Transgressive fluviatile to shallow-marine.|~1670- ~1650 Ma|||Unconformably overlies Calvert Superbasin rocks.|Sandstones, siltstones, dolostones.|03-APR-17
40575|Gun Supersequence|68146|5|Briefly described|p3, p199-200|||The base is the c.1690-1670 Ma Gun unconformity.|||Upper part of Torpedo Creek and Warrina Park Quartzites.|Unconformably overlies Prize Supersequence.||
40575|Gun Supersequence|68732|5|Briefly described|p159, p161, p162, p165 Fig.3, p167-171|Statherian|Statherian|Includes Paradise Creek Formation, Urquhart Shale, Breakaway Shale, Moondarra Siltstone, and Warrina Park Quartzite. Maximum depositional age.|ca. 1674; ca. 1688 Ma.||||Includes stromatolitic bioherms and biostromes.|30-NOV-17
40575|Gun Supersequence|69056|6|Mentioned|p55|||||Mount Isa Group.||Possibly correlated with Lady Clayre Formation.||
40575|Gun Supersequence|69591|5|Briefly described|p27, p39, p42-43, p54|||Mount Isa Province. Includes topmost unit of Deighton Quartzite. Marks the onset of deposition (lower McNamara Group) of the Isa Superbasin.||||Unconformably overlies Yeldham Granite. Is overlain by Loretta Supersequence.||
40575|Gun Supersequence|70657|6|Mentioned|p17|||||||||
40575|Gun Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1675 Ma|||Overlain by the Loretta Supersequence.|Siltstone, carbonaceous shale and dolomite.|
40575|Gun Supersequence|72912|5|Briefly described|p33 Fig.12, p34.|Paleoproterozic|Paleoproterozic|Appear to be affected by oil staining and hence warrant further investigation into their oil or condensate potential.|||Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation and Fish River.|Underlies Loretta Supersequence.||
40575|Gun Supersequence|73144|4|Described|p8-11, p19|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains two third order sequences [see article for more detail on third order sequences]. Deposited below storm wavebase depth in a marine environment (Southgate et al., 2000). Transitions from fluvial and coastal facies in the north and west to progressively peritidal, inner to outer ramp carbonate facies and deeper water, fine-grained siliciclastics and carbonates in the south and east (Southgate et al., 1999). Not considered to contain potential shale gas source rocks (Gorton and Troup, 2018).|1655-1690 Ma|||Includes Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation, and Torpedo Creek Formation.|Siltstone, sandstone and dolomudstone.|
36242|Gunnawarra Bump Granite|23503|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
25038|Gunpowder Creek Formation|22438|4|Described|p539, Fig.3 p537|||Subdivided in Fig.3 into an upper and lower formation. See also Fig.10a p546||||||
25038|Gunpowder Creek Formation|22585|6|Mentioned|Fig3 P738|||Actually spelt Gunpowder Creek Fm.||||||
25038|Gunpowder Creek Formation|22680|6|Mentioned|83,85,87|||Geol province Mount Isa Basin. Parent McNamara Group||||||
25038|Gunpowder Creek Formation|22747|6|Mentioned|Table1,p7|||With Paradise Creek Formation correlates with Suprise Creek Beds and Ploughed Mountain Beds||||||
25038|Gunpowder Creek Formation|23031|5|Briefly described|53|||Geol province Lawn Hill Subprovince. Parent McNamara Group. Overlying unit Paradise Creek Formation, underlying unit Torpedo Creek Quartzite||||||13-AUG-13
25038|Gunpowder Creek Formation|23073|5|Briefly described|p744 (fig 2)|||||||||
25038|Gunpowder Creek Formation|23198|6|Mentioned|p873-876|||||||||
25038|Gunpowder Creek Formation|23362|5|Briefly described|339|||||||||
25038|Gunpowder Creek Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
25038|Gunpowder Creek Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group. Overlies Torpedo Creek Quartzite.||||||13-AUG-13
25038|Gunpowder Creek Formation|23396|4|Described|p419|Statherian|Statherian|Of McNamara Group. 1694+/-3Ma.||||||13-AUG-13
25038|Gunpowder Creek Formation|23397|5|Briefly described|p469|||||||||
25038|Gunpowder Creek Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group. 1694+/-3Ma.||||||
25038|Gunpowder Creek Formation|23399|5|Briefly described|p493 Fig.3|||Of McNamara Group.||||||27-MAY-08
25038|Gunpowder Creek Formation|23406|5|Briefly described|p603, p607 Fig. 8, p611|||Geological province: Lawn Hill Platform. Also referred to as Gunpowder Formation.||||||16-JUN-09
25038|Gunpowder Creek Formation|23408|4|Described|p513 Fig. 2, p514|||Of McNamara Group.||||||15-JUN-09
25038|Gunpowder Creek Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group.||||||01-OCT-08
25038|Gunpowder Creek Formation|23466|5|Briefly described|p267|Statherian|Statherian|1694+/-7Ma||||||
25038|Gunpowder Creek Formation|23518|4|Described|p12|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Western Fold Belt.||||||
25038|Gunpowder Creek Formation|23767|5|Briefly described|p1955|||See also p1957.||||||
25038|Gunpowder Creek Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
25038|Gunpowder Creek Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 800m.||||||
25038|Gunpowder Creek Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
25038|Gunpowder Creek Formation|24033|5|Briefly described|p5|||Includes orthoquartzite, conglomerate, micaceous siltstone and ferruginous siltstone.||||||
25038|Gunpowder Creek Formation|24034|6|Mentioned|p38|||Geological Province: Mount Isa Inlier. Fe-rich litology.||||||
25038|Gunpowder Creek Formation|24156|5|Briefly described|p18|Proterozoic|Proterozoic|Has limited stratabound Zn-Pb-Ag mineralisation at Cowie.|||||Iron-rich sediments.|
25038|Gunpowder Creek Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: McNamara Group||||||07-NOV-08
25038|Gunpowder Creek Formation|24419|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.  Conformably overlies and interfingers with Torpedo Creek Formation.||||||07-NOV-08
25038|Gunpowder Creek Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1694 Ma.||||||
25038|Gunpowder Creek Formation|29969|5|Briefly described|p392|||||||||
25038|Gunpowder Creek Formation|30535|6|Mentioned|p404|||Refer de Keyser(1958)||||||
25038|Gunpowder Creek Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|31207|6|Mentioned|p1414|||||||||
25038|Gunpowder Creek Formation|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|31704|6|Mentioned|p4|||Favourable horizon for copper||||||
25038|Gunpowder Creek Formation|31821|5|Briefly described|p1024|||||||||
25038|Gunpowder Creek Formation|31877|5|Briefly described|p378|||||||||
25038|Gunpowder Creek Formation|32264|4|Described|p386|||See Table 1||||||
25038|Gunpowder Creek Formation|32287|4|Described|p19|||See also p17.||||||13-APR-18
25038|Gunpowder Creek Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|32660|5|Briefly described|Table 5|||||||||
25038|Gunpowder Creek Formation|32959|6|Mentioned|Fig.21|||||||||
25038|Gunpowder Creek Formation|33899|6|Mentioned|p22|||||||||
25038|Gunpowder Creek Formation|33900|6|Mentioned|p15|||||||||
25038|Gunpowder Creek Formation|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|35001|6|Mentioned|Fig.45|||||||||
25038|Gunpowder Creek Formation|35004|6|Mentioned|p266|||||||||
25038|Gunpowder Creek Formation|35074|6|Mentioned|Fig.2|||||||||
25038|Gunpowder Creek Formation|35115|6|Mentioned|p207|||||||||
25038|Gunpowder Creek Formation|35116|6|Mentioned|p186|||||||||
25038|Gunpowder Creek Formation|35167|6|Mentioned|p151|||||||||
25038|Gunpowder Creek Formation|35932|6|Mentioned|p462|||||||||
25038|Gunpowder Creek Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|36548|6|Mentioned|p517|||||||||
25038|Gunpowder Creek Formation|37217|6|Mentioned|p650|||||||||
25038|Gunpowder Creek Formation|37459|1|Redefined|p428|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||01-OCT-08
25038|Gunpowder Creek Formation|37555|6|Mentioned|p3|||||||||
25038|Gunpowder Creek Formation|37568|5|Briefly described|p84|||||||||
25038|Gunpowder Creek Formation|37569|5|Briefly described|p91|||||||||
25038|Gunpowder Creek Formation|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|38232|6|Mentioned|p89|||||||||
25038|Gunpowder Creek Formation|38233|5|Briefly described|Table 1|||||||||
25038|Gunpowder Creek Formation|38237|4|Described|p127|||||||||
25038|Gunpowder Creek Formation|38276|6|Mentioned|Fig.1|||||||||
25038|Gunpowder Creek Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|38348|4|Described|p8|||||||||
25038|Gunpowder Creek Formation|38350|4|Described|p15|||||||||
25038|Gunpowder Creek Formation|38446|5|Briefly described|p187|||||||||
25038|Gunpowder Creek Formation|38584|6|Mentioned|p22|||||||||
25038|Gunpowder Creek Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|38919|6|Mentioned|p496|||||||||
25038|Gunpowder Creek Formation|39445|5|Briefly described|Table 2|||See also p41.||||||13-APR-18
25038|Gunpowder Creek Formation|39497|6|Mentioned|Fig.4|||||||||
25038|Gunpowder Creek Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Overlies Torpedo Creek Quartzite; underlies Paradise Creek Formation.||||||15-JUN-06
25038|Gunpowder Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|39925|6|Mentioned|Fig.9|||||||||
25038|Gunpowder Creek Formation|39943|6|Mentioned|Table 1A|||||||||
25038|Gunpowder Creek Formation|39944|3|Fully described|p233|||||||||
25038|Gunpowder Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|40221|3|Fully described|p14|||||||||
25038|Gunpowder Creek Formation|40394|6|Mentioned|p285|||||||||
25038|Gunpowder Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
25038|Gunpowder Creek Formation|41307|4|Described|p16|||||||||
25038|Gunpowder Creek Formation|41489|6|Mentioned|p516|||||||||
25038|Gunpowder Creek Formation|42166|6|Mentioned|p108|||||||||
25038|Gunpowder Creek Formation|42367|5|Briefly described|p18|||McNamara Group||||||
25038|Gunpowder Creek Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||27-MAY-08
25038|Gunpowder Creek Formation|44115|14|Not recorded|p17|||||||||
25038|Gunpowder Creek Formation|44210|2|Defined|map,Tb.1,p8,9|||||||||
25038|Gunpowder Creek Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|44271|2|Defined|p35,56|||Contains mineral deposits.||||||
25038|Gunpowder Creek Formation|44275|14|Not recorded|Map Legend|||||||||
25038|Gunpowder Creek Formation|44279|14|Not recorded|Tb.1|||||||||
25038|Gunpowder Creek Formation|44290|2|Defined|p438|||Precambrian probably Palaeoproterozoic.||||||
25038|Gunpowder Creek Formation|44521|14|Not recorded|p8,10,21,map|||upper Early Proterozoic||||||
25038|Gunpowder Creek Formation|44552|14|Not recorded|p6,8,9|||||||||
25038|Gunpowder Creek Formation|44989|2|Defined|p.104-7|||On many pages. Tb.III. Penecontemp.with Ploughed Mount. and Surprise Creek Beds. (E54-13,F54-1).||||||25-SEP-06
25038|Gunpowder Creek Formation|45161|5|Briefly described|Table 3|||||||||
25038|Gunpowder Creek Formation|45166|5|Briefly described|p30|||||||||
25038|Gunpowder Creek Formation|45287|14|Not recorded|p.225,226,229||Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25038|Gunpowder Creek Formation|47083|3|Fully described|p15||Proterozoic|Equivalent to Moondarra Siltstone and Breakaway Shale. Of McNamara Gp. Overlain by Paradise Crk Fm; underlain by Torpedo Crk Quartzite. Maximum thickness 800 m.||||||25-SEP-06
25038|Gunpowder Creek Formation|49041|6|Mentioned|Table 4|||||||||
25038|Gunpowder Creek Formation|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
25038|Gunpowder Creek Formation|50550|5|Briefly described|p1139 Fig.2,p1143 Fig.6||Statherian|Age: 1694 Ma. Overlies Torpedo Creek Quartzite at syn-rift unconformity, overlain by Mount Oxide Chert at post-rift unconformity. Geological Province: Western Fold Belt.||||||19-DEC-07
25038|Gunpowder Creek Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Siltstone, sandstone, dolomite.  Overlain by Paradise Creek Formation.||||||
25038|Gunpowder Creek Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metasiltstone. Of the McNamara Group.||||||
25038|Gunpowder Creek Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Paradise Creek Formation.||||||03-JUN-09
25038|Gunpowder Creek Formation|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: ~1694Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
25038|Gunpowder Creek Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Gunpowder Ck Fm.||McNamara Group|||Variably dolomitic organic siltstones and shales.|
25038|Gunpowder Creek Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone and some shales.||||||30-SEP-08
25038|Gunpowder Creek Formation|63111|5|Briefly described|p1162, p1164 Tb. 1|Statherian|Statherian|Of Prize Supersequence. Age: 1690+/-7Ma. Geological Province: Isa Superbasin. Conglomeratic and massive quartzite, sandstone, siltstone, claystone, fine-grained feldspathic sandstone, dolomitic sandstone.||||||07-FEB-11
25038|Gunpowder Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Gun supersequence||||
25038|Gunpowder Creek Formation|63866|5|Briefly described|p57|||Calvert Superbasin.||Gun Supersequence||Overlies the Bigie Formation.||
25038|Gunpowder Creek Formation|63884|5|Briefly described|p14|||Siliciclastic. In contact with Paradise Creek Formation.||||||
25038|Gunpowder Creek Formation|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
25038|Gunpowder Creek Formation|65228|5|Briefly described|p16, Figs.04, 10.|Statherian|Statherian|Contains the maximum flooding surface of the Gun Supersequence, informally named after this unit. Lower part studied in detail by Sami et al. (2000). Age is for the lower part of the unit (in the Prize Supersequence).|1694 +/- 3 Ma.|Unit in McNamara Group.||||
25038|Gunpowder Creek Formation|65337|5|Briefly described|p5, p32, p33 Fig.27.|||Calvert Superbasin. |1694 +/- 3 Ma.|Unit in McNamara Group.||Overlies Surprise Creek Formation. Is overlain by Paradise Creek Formation.|Includes tuffs.|
25038|Gunpowder Creek Formation|66844|5|Briefly described|p243-244,253,254, 264, 271,273|||Lawn Hill Platform. Characterised by a regionally correlative unconformity (Gun Supersequence boundary) in the lower to middle GCF representing a depositional hiatus of 28my, separating the Gun and underlying Prize supersequences. Stromatolites are dominantly domal-columnar, indicative of shallow sub-tidal and peritidal environments.||Of lower McNamara Group; Gun and Prize supersequences.|Informally subdivided into lower and upper parts at Gun and Prize sequence boundaries.||Initially siliciclastic. Includes organic-rich shales and phosphatic precipitates near the top.|
25038|Gunpowder Creek Formation|67323|5|Briefly described|GIS attrib tbl, p10-12, p72|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map. Isa Superbasin. p10 (Century Domain) says Calvert Superbasin and age 1694 +/-3 Ma, p11(Mount Oxide Domain) says age (from adjacent terranes): 1658+/-3 Ma and 1653+/-7 Ma. In Western Fold Belt, contains most of the Ag anomalies. Appears as Upper Gunpowder Formation in the Mount Isa Block Time-Space Plot.||McNamara Group.|||Laminated siltstone, dolomitic and carbonaceous siltstone, fine sandstone, feldspathic and pyritic quartzite, pebbly clayey sandstone.|
25038|Gunpowder Creek Formation|68146|6|Mentioned|p203|||The lower part of this unit contains peperites related to volcanism at c.1694 Ma.||||||
25038|Gunpowder Creek Formation|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlain by Paradise Creek Formation, overlies Torpedo Creek Quartzite||
25038|Gunpowder Creek Formation|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Kamarga Zn-Pb-Ag deposit.||Lower McNamara Group.||Overlies Torpedo Creek Quartzite. Is overlain by Paradise Creek Formation.||
25038|Gunpowder Creek Formation|68732|5|Briefly described|p160-163, p168|||Hosts the Oxide Mine. Undulatory rhythmite facies common. In its lower parts, this formation contains iron-stained and quartz-rich intraclast grainstones, locally with domal and digitate stromatolite bioherms.||||Overlies Torpedo Creek Quartzite. Overlain by the Mount Oxide Chert.|Siliciclastic sediments. Mainly very fine-grained arkosic sandstones.|30-NOV-17
25038|Gunpowder Creek Formation|69591|5|Briefly described|p38 Fig.2.23,p42-44,p49 Fig.2.41,p54,p88|||Is presented on p43 (in Fig.2.31) as Lower and Upper Gunpowder Creek Formations. Part of Gun Supersequence. Shallow-marine deposits. Is lithologically similar to Moondarra Siltstone (Mount Isa Group).||McNamara Group.||Overlies Torpedo Creek Quartzite. Unconformably overlies Myally Subgroup.|Laminated siltstone, dolomitic and carbonaceous siltstone, fine sandstone, feldspathic and pyritic quartzite, pebbly clayey sandstone.|
25038|Gunpowder Creek Formation|70864|5|Briefly described|p75, 74 Fig 2, p79, 81, 82|Mesoproterozoic||||McNamara Group|Overlain by Surprise Creek Formation||Siltstones, shales and sandstones.|
25038|Gunpowder Creek Formation|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1689+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Chert, sandstone, tuff.|
25038|Gunpowder Creek Formation|72912|5|Briefly described|p33 Fig.12.|Paleoproterozic|Paleoproterozic|Shown as part of McNamara Group.||||Underlies Paradise Creek Formation|Includes dolostone.|
25038|Gunpowder Creek Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.||McNamara Group||Underlies Paradise Creek Formation.|Includes dolostone.|
25038|Gunpowder Creek Formation|72919|4|Described|p56-57, p63|Statherian|Statherian|Mount Isa Province. [Also written as 'Gunpowder Creek Formation']. Lithological description from Southgate et al. (1999). Deposited between ca. 1694 Ma and ca. 1658 Ma. Tuff crystallisation age of ca. 1694 Ma reported by Page et al. (2000). An internal unconformity has been inferred, although Withnall and Hutton (2013) suggested the portion containing glauconitic sandstones and finer units in Morstone 1 may instead correlate to the Mullera Formation.|Between ca. 1694 Ma and ca. 1658 Ma||||Thin-bedded to laminated siltstone and shale, with minor sandstone, dolostone and chert.|
25038|Gunpowder Creek Formation|73144|6|Mentioned|p9|||Isa Superbasin. Part of the Gun Supersequence.||||||
25038|Gunpowder Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1703+/-15 Ma MDA, 1694+/-3 Ma age of volcanic rock||||Clastics.|
30696|Guns Knob Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30696|Guns Knob Granite|50536|5|Briefly described|p1.4, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30696|Guns Knob Granite|63023|6|Mentioned|p1035 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1674+/-4Ma (SHRIMP U-Pb). Coarse-grained, phenocrystic granite in the central-eastern part of the main Sybella Granite body.||||||07-NOV-08
30696|Guns Knob Granite|64744|6|Mentioned|p357 Table 1. |Statherian|Statherian|Central Sybella region. Moderately gneissic.|1674 +/- 4 Ma.|||||
30696|Guns Knob Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Mount Isa Block Time-Space Plot. Sybella Domain, Mount Isa Inlier. Sybella Igneous Event.|1674 +/- 4 Ma.|Sybella Suite.|||Variably porphyritic medium to coarse biotite granite.|
30696|Guns Knob Granite|69591|5|Briefly described|p59|||Sybella Batholith.|1674 +/- 4 Ma (Neumann et al., 2006).||||Variably porphyritic medium to coarse biotite granite.|
30696|Guns Knob Granite|71592|5|Briefly described|Appendix A.|||Sybella Domain, Mount Isa Orogen.|1674+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
23640|Guymer Trachyte Member|39969|6|Mentioned|p9|||||||||
23640|Guymer Trachyte Member|40542|6|Mentioned|p98|||||||||
23640|Guymer Trachyte Member|73450|6|Mentioned|p92|||Of Stevens, 1965; Grenfell, 1984; Ewart & Grenfell, 1985. Never described in detail.||Governors Chair Volcanics|||Felsic.|29-SEP-22
36222|Gyp Swamp Granodiorite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Possibly intrudes Tate Batholith undivided. Geological Province: Georgetown Region.||||||08-JUL-15
36222|Gyp Swamp Granodiorite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36222|Gyp Swamp Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 365. I-Type.||||||
36222|Gyp Swamp Granodiorite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
40990|Gyranda Subgroup|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Erroneously presented as part of Back Creek Group. Contains the Banana Formation and the Wiseman Formation.||||||10-NOV-05
40990|Gyranda Subgroup|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Blackwater Group. Includes the Banana and Wiseman Formations.||||||18-MAY-04
40990|Gyranda Subgroup|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Blackwater Group.||||||
40990|Gyranda Subgroup|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Back Creek Group (incorrect parentage?).||||||10-NOV-05
40990|Gyranda Subgroup|65388|4|Described|p193-196, 48, 70, 161, 163, 171, 174,439|Early Triassic|Late Permian|Bowen Basin. A non-marine succession conformably overlying the Flat Top Formation (Back Creek Group) and conformably overlain by the Baralaba Coal Measures and herein raised in status to Gyranda Subgroup including the Banana and Wiseman Formations. GSQ Mundubbera 5 from 214-879m is a reference section. Mudstone, lithic sandstone (locally calcareous), fine-grained tuff, minor siltstone and rare conglomerate and volcanic breccia.||||||
40990|Gyranda Subgroup|68679|6|Mentioned|p308|Permian|Permian|Bowen Basin.||||||
40990|Gyranda Subgroup|73450|6|Mentioned|p55|||Bowen Basin.||||||
32149|Hainault Granodiorite|23037|5|Briefly described|p74,84,5|Early Permian|Silesian|||||||
32149|Hainault Granodiorite|65388|4|Described|p258, 236 Fig.81, 237-8, 248, 252-3, 259|Early Permian|Late Carboniferous|Auburn Arch. Interpreted as older than Dawson Granite. Similar lithology to Glandore Granodiorite and  Hildura Quartz Monzodiorite. Relationships not clear. Dark grey medium-grained hornblende-biotite granodiorite or quartz monzodiorite. Age assigned tentatively, but may be mid-Carboniferous like Glandore Granodiorite.||||||
32149|Hainault Granodiorite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Quartz monzonite resembles Glandore Granodiorite and may be of similar age (middle Carboniferous). Relationships to surrounding units unclear.|||||Mostly hornblende-biotite granodiorite or quartz monzodiorite.|
26603|Hales Siding Granite|23423|6|Mentioned|p306 Table 7.3|||||||||
26603|Hales Siding Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite. Age: ~314Ma Rb-Sr.||||||01-JUN-09
26603|Hales Siding Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 279. I-Type.||||||
26603|Hales Siding Granite|23616|6|Mentioned|Table 3 p48|||||||||
26603|Hales Siding Granite|33205|6|Mentioned|Map legend|Permian|Permian|Probably Permian.||||||01-JUN-09
26603|Hales Siding Granite|39445|6|Mentioned|p90|||Blake(1972)||||||
26603|Hales Siding Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supersuite).  Pale pink, fine to medium-coarse, even-grained biotite granite and leucogranite.Age: 313Ma.||||||15-JUN-06
26603|Hales Siding Granite|43259|4|Described|Appendix 1,p35.||Carboniferous|Age is 313 Ma.||||||
26603|Hales Siding Granite|43626|6|Mentioned|p10||Late Carboniferous|||||||
26603|Hales Siding Granite|45065|4|Described|Table 4|||||||||
26603|Hales Siding Granite|45113|3|Fully described|p13|||Emphasis on petrography.||||||
26603|Hales Siding Granite|46845|6|Mentioned|Table 1|||||||||
26603|Hales Siding Granite|46879|6|Mentioned|Fig.1|||||||||
26603|Hales Siding Granite|60425|4|Described|p49 Tb.3, p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supersuite). Intruded Boonmoo Volcanic Subgroup.Pale pink, fine- to coarse-grained, even-grained, biotite granite and leucogranite; minor slightly porphyritic hornblende-biotite granite;rare aplitic microgranite; I-type.||||||07-FEB-11
79131|Hall Clastics Member|70913|4|Described|p52-56, p8 fig 3, p11, App 1 maps|Middle Permian|Early Permian|Gympie Province. Previously Hall Clastics/clastics. Also abbreviated to Hall Clastics, p41, 44, 49, 52, 56. Named for the Hall Road near the West of Scotland shaft. No outcrop references are known and only one complete drill hole intersects this member; this drill hole does not represent typical lithologies of this unit. Up to 200m thick in the Monkland block. Distribution is discussed briefly. The conglomerate of this Memberis intruded by the Tozer Basalt. See also p45 fig 6, p67 fig 9. See also Hall Group p12 [a probable equivalent].||Dawn Formation||Intruded by Tozer Basalt. Overlies the Ellen Harkins Shale[?]. Overlain by the Kidgell Andesite Member [?].|Medium to coarse-grained, volcanoclastic sedimentary rocks or pyroclastic deposits including green volcanogenic conglomerate, basalt and andesite clasts, hyaloclastite and siltstone.|27-FEB-19
25720|Halls Reward Metamorphics|22533|6|Mentioned|p54,p56|||||||||
25720|Halls Reward Metamorphics|23032|5|Briefly described|p12,50|||Thought to be Proterozoic.||||||
25720|Halls Reward Metamorphics|23220|6|Mentioned|Fig.1|||of Georgetown Inlier.||||||
25720|Halls Reward Metamorphics|23291|4|Described|p27, p83 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Region.||||||08-JUL-15
25720|Halls Reward Metamorphics|23424|5|Briefly described|Table 8.1 p327 p331||Proterozoic|Faulted against Judea Formation. Forsayth Subprovince/Etheridge Province.||||||
25720|Halls Reward Metamorphics|23430|5|Briefly described|p450|||Forsayth Sub-province. Etheridge Province.||||||
25720|Halls Reward Metamorphics|23431|5|Briefly described|p530|||Etheridge Province.||||||
25720|Halls Reward Metamorphics|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25720|Halls Reward Metamorphics|23498|6|Mentioned|p25 table 1|||||||||
25720|Halls Reward Metamorphics|23503|5|Briefly described|Map Legend||Mesoproterozoic|||||||
25720|Halls Reward Metamorphics|23616|4|Described|Table 1C p16, p28||Proterozoic|Age: Early or Middle Proterozoic. Intruded by granitoids of the Tirrabella Supersuite and Permo-Carboniferous granitoids; unconformably overlain by Cainozoic McBride Basalt. Hodgkinson Province.||||||04-JUL-14
25720|Halls Reward Metamorphics|23619|4|Described|p37 Table 1||Proterozoic|Intruded by Boiler Gully Complex and Dido Tonalite.  Georgetown Province.||||||
25720|Halls Reward Metamorphics|24577|5|Briefly described|p755 Fig. 2|Early Paleozoic|Proterozoic|Geological Province: Lachlan Fold Belt.||||||07-NOV-08
25720|Halls Reward Metamorphics|29446|4|Described|p123|||See also P120||||||
25720|Halls Reward Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25720|Halls Reward Metamorphics|31832|6|Mentioned|Table 6|||||||||
25720|Halls Reward Metamorphics|32528|5|Briefly described|Table 1|||||||||
25720|Halls Reward Metamorphics|32553|4|Described|p54|||||||||
25720|Halls Reward Metamorphics|33669|6|Mentioned|p517|||||||||
25720|Halls Reward Metamorphics|34013|6|Mentioned|Fig.1|||Archaean||||||
25720|Halls Reward Metamorphics|35921|6|Mentioned|Fig.2|||||||||
25720|Halls Reward Metamorphics|35948|6|Mentioned|Fig.1|||||||||
25720|Halls Reward Metamorphics|37570|4|Described|p112|||See also p109.||||||03-SEP-18
25720|Halls Reward Metamorphics|37571|4|Described|p137|||||||||
25720|Halls Reward Metamorphics|37768|5|Briefly described|p34|||||||||
25720|Halls Reward Metamorphics|37769|6|Mentioned|p47|||||||||
25720|Halls Reward Metamorphics|39027|6|Mentioned|Map legend|Archean|Archean|Prob. Archaean||||||07-NOV-08
25720|Halls Reward Metamorphics|39445|5|Briefly described|p45|||See also Table 2||||||
25720|Halls Reward Metamorphics|39687|6|Mentioned|p1|||||||||
25720|Halls Reward Metamorphics|39689|6|Mentioned|Fig.2|||||||||
25720|Halls Reward Metamorphics|40787|6|Mentioned|p324|||||||||
25720|Halls Reward Metamorphics|40961|6|Mentioned|p239|||||||||
25720|Halls Reward Metamorphics|41260|6|Mentioned|p110|||||||||
25720|Halls Reward Metamorphics|41675|1|Redefined|p12|Archean||||||||07-NOV-08
25720|Halls Reward Metamorphics|41719|6|Mentioned|p215|||||||||
25720|Halls Reward Metamorphics|41916|6|Mentioned|p26|||||||||
25720|Halls Reward Metamorphics|41975|6|Mentioned|p439|||||||||
25720|Halls Reward Metamorphics|42054|6|Mentioned|p273|||||||||
25720|Halls Reward Metamorphics|42199|5|Briefly described|Table 1 P280|||||||||
25720|Halls Reward Metamorphics|42279|5|Briefly described|p17|||See also Fig.2||||||
25720|Halls Reward Metamorphics|42407|5|Briefly described|p33|||||||||
25720|Halls Reward Metamorphics|42692|5|Briefly described|map legend|Proterozoic||||||||
25720|Halls Reward Metamorphics|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
25720|Halls Reward Metamorphics|42747|6|Mentioned|p35|||||||||
25720|Halls Reward Metamorphics|42933|5|Briefly described|p46|||||||||
25720|Halls Reward Metamorphics|43060|3|Fully described|p35,Table 1c|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
25720|Halls Reward Metamorphics|43113|4|Described|Table 1 p23||Proterozoic|||||||
25720|Halls Reward Metamorphics|43213|6|Mentioned|p9, p62|||Near Greenvale, Broken River Province; also eastern Georgetown Province.||||Faulted against Wairuna Formation.||
25720|Halls Reward Metamorphics|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
25720|Halls Reward Metamorphics|43286|5|Briefly described|Map Legend||Proterozoic|||||||
25720|Halls Reward Metamorphics|43480|6|Mentioned|13|||||||||
25720|Halls Reward Metamorphics|43664|6|Mentioned|p83||Mesoproterozoic|||||||
25720|Halls Reward Metamorphics|43716|6|Mentioned|p17|||||||||
25720|Halls Reward Metamorphics|43729|5|Briefly described|p3||Proterozoic|||||||
25720|Halls Reward Metamorphics|44043|14|Not recorded|Tb.1,Fig.8,p67,70,73||Proterozoic|Overlies Stenhouse Creek Amphibolite. Unconformably overlain by Paddys Creek Formation. Intruded by Sandalwood Serpentinite.||||||
25720|Halls Reward Metamorphics|44048|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
25720|Halls Reward Metamorphics|44059|2|Defined|p443,446||Archean|||||||07-NOV-08
25720|Halls Reward Metamorphics|44246|5|Briefly described|Map Legend||Proterozoic|||||||
25720|Halls Reward Metamorphics|44258|14|Not recorded|p30||Archean|||||||07-NOV-08
25720|Halls Reward Metamorphics|45009|2|Defined|p21,25-28,31,32,79,||Archean|p115,Tb.2,Pl.13||||||07-NOV-08
25720|Halls Reward Metamorphics|45151|5|Briefly described|Table 4|||||||||
25720|Halls Reward Metamorphics|48904|14|Not recorded|p127 and map|||Possible correlation with Argentine Metamorphics.||||||
25720|Halls Reward Metamorphics|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|Mica schist, biotite gneiss and pegmatite; locally mylonitised.||||||07-NOV-08
25720|Halls Reward Metamorphics|63866|5|Briefly described|p78-p79, p82|||Shear-hosted copper deposits occur within this unit.||||||
25720|Halls Reward Metamorphics|65380|6|Mentioned|p679|||Georgetown Province.||||||27-MAR-12
25720|Halls Reward Metamorphics|65887|5|Briefly described|p40 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
25720|Halls Reward Metamorphics|67455|4|Described|p573, p575 Table 1,  p576, p577, p563. |Ordovician|Cambrian|Halls Reward domain. Has detrital zircons aged 600 Ma. Deformed by the Delamerian Orogeny at 510 - 500 Ma. May represent a basement block upstanding as a horst during Early Ordovician extension, and not influenced by ductile deformation that affected deeper levels of the adjacent backarc basin. Has one main foliation, east-west striking and dipping steeply to the north.|510-500 Ma (K-Ar and Rb/Sr: Nishiya et al. 2003).||||Coarse-grained muscovite-quartz schist with biotite, sillimanite and garnet; abundant leucogranite and pegmatite.|
25720|Halls Reward Metamorphics|67848|5|Briefly described|p4, p5 Fig.3. |Neoproterozoic|Neoproterozoic|Greenvale Province. Intercalated with meta-igneous rocks of mafic-ultramafic association (Boiler Gully Complex).||||||
25720|Halls Reward Metamorphics|68336|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||||Mica schist, biotite gneiss and pegmatite; includes some unmapped Stenhouse Creek Amphibolite; locally mylonitised.|
25720|Halls Reward Metamorphics|68341|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.|||||Mica schist, biotite gneiss and pegmatite; includes some unmapped Stenhouse Creek Amphibolite; locally mylonitised.|
25720|Halls Reward Metamorphics|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Cape River Province. Weakly to non-magnetic.|||||Mica schist, biotite gneiss and pegmatite; locally mylonitised.|
25720|Halls Reward Metamorphics|68480|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Cape River Province. Neoproterozoic? maximum age.|||||Mica schist, biotite gneiss and pegmatite; some amphibolite; locally mylonitised.|
25720|Halls Reward Metamorphics|68481|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Cape River Province. Neoproterozoic? to Cambrian? in age.|||||Mica schist, biotite gneiss and pegmatite; some amphibolite; locally mylonitised.|
25720|Halls Reward Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Greenvale Province.||||||
25720|Halls Reward Metamorphics|68576|5|Briefly described|Q_11: p34-35, p40|||Greenvale area. Forms a metasedimentary tract on the edge of the Greenvale Province. Neoproterozoic or Early Cambrian protoliths were deformed in the Middle Cambrian (520-500 Ma: Nishiya et al., 2003).|||||Includes mica schist. Amphibolite facies metamorphism.|
25720|Halls Reward Metamorphics|68731|5|Briefly described|p152, p155, p156, p158, p159, p189, p218|Middle Cambrian|Neoproterozoic|Greenvale Province. Age data confirms a latest Neoproterozoic or early Paleozoic age and not Mesoproterozoic as previously thought.||||Nonconformably overlain by the Blue Rock Creek beds.||04-JUL-14
25720|Halls Reward Metamorphics|68822|6|Mentioned|p323|||||||||
25720|Halls Reward Metamorphics|69592|5|Briefly described|p250, p252|Proterozoic|Proterozoic|Broken River Province.||||Is intruded by or is tectonically intercalated with Boiler Gully Complex.||
25720|Halls Reward Metamorphics|70033|6|Mentioned|p52 Fig 8.1||Neoproterozoic|Thomson Orogen. Age shown in map legend (Fig 8.1) as Neoproterozoic - Cambrian?||||||
25720|Halls Reward Metamorphics|70207|5|Briefly described|p1, p11, p20, p31-37|Paleozoic|Neoproterozoic|Greenvale Province, Thomson Orogen. Maximum depositional age; younger than previous metamorphism age (510-500 Ma: Nishiya et al., 2003) which may have been detrital zircons. This ~474 Ma age suggests this unit may belong to the Broken River Province or the Mossman Orogen rather than the Thomson Orogen.|474.2 +/- 5.8 Ma (Kositcin et al., 2015).||||Amphibolite facies mica schist, quartzite, biotite-muscovite gneiss, and metamorphosed mafic and ultramafic rocks.|
25720|Halls Reward Metamorphics|70744|5|Briefly described|p939|||Greenvale Province. K/Ar age by Nishiya et al. (2003).|c.500 Ma (estimated from Fig.7).|||||
25720|Halls Reward Metamorphics|70749|5|Briefly described|p42-43|Cambrian|Cambrian|Greenvale Province.|~474 Ma (maximum depositional age).|||||
25720|Halls Reward Metamorphics|71031|5|Briefly described|p3-p4, p6, p13, p62-p63, p65-p68|||Thomson Orogen, Greenvale Province. Potentially belongs to the Broken River Province and Mossman Orogen. An additional maximum depositional age of 474.2 +/- 5.8 Ma for a sample of quartz-muscovite schist was reported in Kositcin et al, 2015a.|459.5 +/- 4 Ma SHRIMP U-Pb (Max dep.)||||Amphibolite facies mica schist, quartzite, biotite-muscovite gneiss and metamorphosed mafics and ultramafics.|
25720|Halls Reward Metamorphics|71592|5|Briefly described|Appendix A.|||Greenvale Province, Thomson Orogen.|474+/-5.8 Ma (MDA: U-Pb zircon SHRIMP)||||Schist.|
25720|Halls Reward Metamorphics|71966|6|Mentioned|p990|Ordovician|Ordovician|Geological province: Greenvale Province, Thomson Orogen. |<474 Ma|||||
25720|Halls Reward Metamorphics|73425|6|Mentioned|p2, 16|Middle Cambrian|Middle Cambrian|Greenvale Province, Thomson Orogen.||||||
79464|Hamilton River Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Granitoid: interpreted from magnetic data.|
79464|Hamilton River Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Interpreted from subsurface and magnetic data only.||Williams Supersuite|||Granitoid? Interpreted from magnetic data.|20-JAN-22
79464|Hamilton River Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Interpreted from magnetic data.||Williams Supersuite|||Granitoid?
|
36295|Hammock Creek Rhyolite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Scardons Volcanic Group.||||||27-AUG-04
76907|Hampden Slate|67323|5|Briefly described|GIS attrib tbl, p18-19|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin.||Kuridala Group.||Correlated with Toole Creek Volcanics. Age-equivalent to Answer Slate.|Graphitic slate and metasiltstone; minor schist, calcareous and banded calc-silicate rocks; numerous metadolerite sills.|
76907|Hampden Slate|69056|5|Briefly described|p55|||||Topmost Kuridala Group.||Overlies New Hope Sandstone. Equivalent to Toole Creek Volcanics.|Includes metadolerite sills.|
76907|Hampden Slate|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Kuridala Group|||Dark grey, carbonaceous slate and metasiltstone; minor schist and calcareous and banded calc-silicate rocks|
76907|Hampden Slate|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Kuridala Group|||Dark grey, carbonaceous slate and metasiltstone; minor schist and calcareous and banded calc-silicate rocks|
76907|Hampden Slate|69591|5|Briefly described|p41, p43, p46, p55|||Kuridala-Selwyn Domain, Calvert Superbasin. Probably coeval with Answer Slate. Part of Gun Supersequence. Deep-marine deposits.||Topmost Kuridala Group.||Overlies New Hope Sandstone. Correlated with Toole Creek Volcanics.|Graphitic slate and metasiltstone; minor schist, calcareous and banded calc-silicate rocks.|
76907|Hampden Slate|69952|5|Briefly described|p2 Tb.i, p4, p51-54|||Mount Isa Province (North Australia Craton). Previous correlation with Toole Creek Volcanics (Soldiers Cap Group) appears to be precluded by these data. SHRIMP U-Pb zircon magmatic crystallisation age of rhyolitic ignimbrite; this age is within error of the maximum depositional age of 1686 +/- 7 Ma obtained by Lambeck (2011) for sandstone in the unit. The ignimbrite used for dating appears to be subaerial; this is at odds with the deep-water marine environment interpreted for the Kuridala Group; thus the relationship of the ignimbrite to its surrounding rocks also needs reassessing.|1684.5 +/- 5.0 Ma (Cross et al., 2015).|Unit in upper part of Kuridala Group.|||Dominantly cleaved carbonaceous mudstone and fine-grained schist; includes sandstone and a belt of rhyolitic volcaniclastic rocks; is intruded by numerous metadolerite and metagabbro sills.|
76907|Hampden Slate|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Kuridala Group.||Overlies New Hope Sandstone. Probable equivalent to Answer Slate.|Dark grey, carbonaceous slate and metasiltstone; minor schist, calcareous and banded calc-silicate rocks.|05-MAY-16
76907|Hampden Slate|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala- Selwyn Domain. ||Kuridala Group.|||Dark grey carbonaceous slate and metasiltstone; minor schist, calcareous and banded calc silicate rocks.|
76907|Hampden Slate|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.||Kuridala Group.|||Dark grey carbonaceous slate and metasiltstone; minor schist and calcareous and banded calc-silicate rocks.|20-JAN-22
76907|Hampden Slate|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.||Kuridala Group |||Carbonaceous slate and metasiltstone; minor schist, calcareous and banded calc-silicate rocks.|
76907|Hampden Slate|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1685+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
76907|Hampden Slate|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kuridala-Selwyn Domain.||Kuridala Group||Overlies New Hope Sandstone.|Dark grey, carbonaceous slate and metasiltstone; minor schist and calcareous and banded calc-silicate rocks.|
76907|Hampden Slate|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kuridala-Selwyn Domain.||Kuridala Group||Overlies New Hope Sandstone.|Dark grey, carbonaceous slate and metasiltstone; minor schist and calcareous and banded calc-silicate rocks.|
76907|Hampden Slate|72889|4|Described|p2-3, p5, p8, 33, 50, 53-60|Statherian|Statherian|Refer to 1:250 000 sheet DUCHESS (SF5406). This age younger than previous reports e.g. magmatic crystallisation age from 'rhyolitic ignimbrite' sample that has been dated at 1684.5 +/- 5.0 Ma, but this subsequently re-interpreted to 1657+/-12 Ma, to account for inherited zircon. Also note previous max. dep. age dating, 1676+/-5 Ma (Neumann and Fraser, 2007) of what was then thought to be Hampden Slate and is now thought to be upper Starcross Formation. Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results.|1650+/-8 Ma max. dep. age, SHRIMP.|Kuridala Group||Conformably overlies Starcross Formation. Intruded by Squirrel Hills Granite.|Sample: Fine to medium-grained, thin to thickly bedded, laminated, quartzose-feldspathic sandstone. General: Carbonaceous and phyllitic rocks.|
76907|Hampden Slate|73525|6|Mentioned|p4-5 Fig.2|||Kuridala-Selwyn-Marimo-Doherty Domain.|||||Carbonaceous shale (-silt) siliciclastics.|
36155|Hann Creek Basalt|23505|5|Briefly described|Map legend||Quaternary|||||||
36155|Hann Creek Basalt|69599|5|Briefly described|p594|Pleistocene|Pleistocene||1.42-1.27 Ma.|||Overlies the Campaspe Formation.||
36155|Hann Creek Basalt|73115|6|Mentioned|p: 75, p77-78|Pleistocene|Pleistocene|[Also written as Hann Creek Basalt Flow in all diagrams]. Nulla Basalt Province.|1.27-1.39 Ma|||Underlain by Campaspe Formation.||
25942|Hardwick Formation|23291|6|Mentioned|p37|Devonian|Devonian|Geological Province: Georgetown Region.||||||08-JUL-15
25942|Hardwick Formation|23422|5|Briefly described|p180, p205 Table 6.3|Early Carboniferous|Late Devonian|Of Keelbottom Group.||||||
25942|Hardwick Formation|23424|5|Briefly described|p337|Early Carboniferous|Late Devonian|Similar age to Teddy Mount Formation (Bundock Basin). Conodonts suggest a Late Devonian (latest) (Famennian) age for the unit. May range up into the E. Carboniferous. Burdekin Basin Province.||||||
25942|Hardwick Formation|23430|5|Briefly described|Plate 14.11|||Of Keelbottom Group. Burdekin Basin Province.||||||
25942|Hardwick Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Keelbottom Group.||||||
25942|Hardwick Formation|23522|5|Briefly described|p250 Fig 6|Early Carboniferous|Early Carboniferous|||||||
25942|Hardwick Formation|23893|5|Briefly described|p16|Early Carboniferous|Late Devonian|Of Keelbottom Group.  Geological Province: Burdekin Basin.||||||
25942|Hardwick Formation|24074|5|Briefly described|p390|Early Carboniferous|Late Devonian|Maximum thickness: 825m.  Geological Province: Clarke River Basin.||||||
25942|Hardwick Formation|24577|4|Described|p752 Fig. 1, p755 Fig. 2|Tournaisian|Tournaisian|Of the Keelbottom Group. Overlain by the Piccadilly Formation. Overlies the Lollypop Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
25942|Hardwick Formation|24613|1|Redefined|p66-67|Tournaisian|Famennian|Includes St Michael Member.||||||07-FEB-11
25942|Hardwick Formation|24614|4|Described|p191 Fig. 1, p199-200|Tournaisian|Tournaisian|Of Keelbottom Gp. Includes Saint Michael Mbr. Consists of feldspathic Sst, subordinate micaceous Mst + calcareous Sst, with minor Lmt + rare pebbly Sst. Max. thickness: 1320m. Geol Prov: Burdekin Basin. See also p193 Fig. 2, p196 Fig. 5.||||||07-FEB-11
25942|Hardwick Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
25942|Hardwick Formation|31285|4|Described|p81|||See also P82, 88. Tournaisian||||||
25942|Hardwick Formation|31999|6|Mentioned|Table 11|||||||||
25942|Hardwick Formation|32140|5|Briefly described|p7|||L.Carboniferous||||||
25942|Hardwick Formation|32169|6|Mentioned|Table 2|||U.Dev.-L.Carb.||||||
25942|Hardwick Formation|32553|4|Described|p48|||||||||
25942|Hardwick Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Early Carboniferous to Late Devonian||||||
25942|Hardwick Formation|36628|6|Mentioned|p24|||||||||
25942|Hardwick Formation|37573|3|Fully described|p218|Tournaisian||See also Figs.14 & 21||||||
25942|Hardwick Formation|38215|6|Mentioned|p275|||||||||
25942|Hardwick Formation|39445|5|Briefly described|Table 6|||||||||
25942|Hardwick Formation|39686|6|Mentioned|p72|||||||||
25942|Hardwick Formation|39735|6|Mentioned|p18|||||||||
25942|Hardwick Formation|42547|4|Described|p66|||||||||
25942|Hardwick Formation|42689|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25942|Hardwick Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25942|Hardwick Formation|42933|5|Briefly described|Fig.94 p258|||||||||
25942|Hardwick Formation|43095|5|Briefly described|Plate 2|||of Keelbottom Group||||||
25942|Hardwick Formation|43933|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Of Keelbottom Group.||||||
25942|Hardwick Formation|44058|14|Not recorded|p103,Tb.p104|||||||||
25942|Hardwick Formation|44060|14|Not recorded|Map Legend|Early Carboniferous|Late Devonian|||||||
25942|Hardwick Formation|44061|14|Not recorded|Table 2|Early Carboniferous|Late Devonian|||||||
25942|Hardwick Formation|44091|14|Not recorded|p46,Tb.3||Early Carboniferous|||||||
25942|Hardwick Formation|44360|14|Not recorded|p28,29|||||||||
25942|Hardwick Formation|45097|6|Mentioned|p22|||Overlies Hardwick Fm. Correlation chart||||||
25942|Hardwick Formation|45151|5|Briefly described|Table 6|||See also P11.||||||
25942|Hardwick Formation|46845|6|Mentioned|Table 1|||||||||
25942|Hardwick Formation|48904|2|Defined|p28|Early Carboniferous|Late Devonian|See also P29. Upper Devonian - Lower Carboniferous||||||
25942|Hardwick Formation|65214|6|Mentioned|p281|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25942|Hardwick Formation|67402|4|Described|p239, p246, p247, p248|Tournaisian|Famennian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a variety of settings including shoreline, nearshore, shelf or marine shoal environments. ||||Overlies the Lollypop Formation. Overlain by the Piccadilly Formation.|Fine-grained sandstone, siltstone, mudstone and limestone alternating with coarser-grained sandstone, pebbly sandstone and minor siltstone.|
25942|Hardwick Formation|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Lollypop Formation.|Lithic to feldspathic sandstone, mudstone, siltstone, conglomerate, fossiliferous sandy limestone and calcilutite and cherty mudstone; marine and plant fossils.|
25942|Hardwick Formation|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Lollypop Formation.|Lithic to feldspathic sandstone, mudstone, siltstone, conglomerate, fossiliferous sandy limestone and calcilutite and cherty mudstone; marine and plant fossils.|
25942|Hardwick Formation|68419|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.||Of the Keelbottom Group.||Conformably overlain by the Piccadilly Formation. Conformably underlain by the Lollypop Formation.|Lithic to feldspathic sandstone, mudstone, siltstone, conglomerate and calcilutite and cherty mudstone; marine and plant fossils.|
25942|Hardwick Formation|68420|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.||Of the Keelbottom Group.||Conformably overlain by the Piccadilly Formation. Conformably underlain by the Lollypop Formation.|Lithic to feldspathic sandstone, mudstone, siltstone, conglomerate and calcilutite and cherty mudstone; marine and plant fossils.|
25942|Hardwick Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4, p187|Mississippian|Mississippian|Burdekin Basin. < 1320 m thick. Shelly beds common. Rare limestone horizons, some oolitic. Three transgressive-regressive cycles are recognised. Diverse benthic fauna with brachiopods, molluscs, crinoids, and rugose corals. Tuffs occur in the upper part.||Of the Keelbottom Group.|Includes the Saint Michael Member.||Comprises very fine grained to medium-grained, less commonly coarse-grained to pebbly labile sandstone, sporadically calcareous with interbeds of micaceous siltstone and mudstone.|
25942|Hardwick Formation|69591|6|Mentioned|p103|Famennian|Famennian|Draper and Lang (1994).||||||
69009|Harkness Granodiorite|61087|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Eidsvold Complex. Pale grey to white, coarse-grained hornblende granodiorite to diorite, locally intermingled with dark grey diorite and gabbro (zones of magma mixing).||||||
69009|Harkness Granodiorite|64399|5|Briefly described|Map legend|Late Permian|Late Permian|Part of the Eidsvold Complex. Coarse-grained hornblende granodiorite, locally intermingled with diorite (zones of magma mixing).||||||05-SEP-14
69009|Harkness Granodiorite|65388|3|Fully described|p292-293, 289, 291, 300|Early Permian|Early Permian|New unit within Eidsvold Complex. Intimately mixed with Mount Rose Gabbro. Tonalite or quartz diorite to granodiorite. Forms an extensive net-vein complex with angular to rounded diorite or gabbro xenoliths/enclaves common. ||||||
69009|Harkness Granodiorite|68679|5|Briefly described|p408|Permian|Permian|Auburn Subprovince, New England Orogen.||Eidsvold Complex.||Intimately mixed with Mount Rose Gabbro.|Fine- to medium-grained tonalite or quartz diorite to granodiorite, forming an extensive net-vein complex with angular to rounded diorite or gabbro xenoliths/enclaves that have dark, fine-grained, crenulated or embayed margins.|
36320|Harpers Tonalite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
36320|Harpers Tonalite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Almaden Supersuite.|||Dark grey, mainly medium-grained, moderately porphyritic hypersthene-augite-hornblende-biotite tonalite; with mafic enclaves up to ~45 cm across.|
24305|Harpur Creek Member|40247|4|Described|p211|||||||||
24305|Harpur Creek Member|40954|6|Mentioned|p133|||||||||
24305|Harpur Creek Member|42975|6|Mentioned|Fig.2 p257|||of Lowmead Formation||||||
24305|Harpur Creek Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably overlain by the Wheatley Oil Shale Member. Conformably underlain by the Hobble Creek Member.|Dominantly calcareous claystone interbedded with siltstone and sandstone; minor oil shale.|
24305|Harpur Creek Member|68421|5|Briefly described|Map Legend|Eocene|Eocene|Lowmead Graben.||Of the Lowmead Formation.||Conformably overlain by the Wheatley Oil Shale Member. Conformably underlain by the Hobble Creek Member.|Dominantly calcareous claystone interbedded with siltstone and sandstone; minor oil shale.|
24305|Harpur Creek Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. 6.5 - 149.7m thick (average 46.1m); oil shale marker bed ranges from 3.8m to 149.7m, averaging 10m.||Lowmead Formation.||Overlies Hobble Creek Member. Is overlain by Wheatley Shale Member.|Interbedded claystone, sandstone and oil shale; a marker oil shale bed.|
32152|Harrami Igneous Complex|23037|4|Described|p86,7||Permian|||||||
32152|Harrami Igneous Complex|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRghr].  Light to dark grey, medium-grained biotite-monzodiorite and light grey, fine- to medium-grained biotite granite; locally mingled with dark grey, medium-grained hornblende gabbro.||||||
32152|Harrami Igneous Complex|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
32152|Harrami Igneous Complex|60282|6|Mentioned|p21|||||||||
32152|Harrami Igneous Complex|65388|2|Defined|p318-319, 39, 237, 238,  301, 338, 340|Permian|Permian|Intrudes and has hornfelsed Camboon Volcanics. May intrude Yaparaba Volcanics. Appears to be intruded by Wingfield Granite, so Permian age assigned. Outcrop poor. Monzodiorite and hornblende gabbro most abundant, but granite and granodiorite locally mingled. Also abbreviated as Harrami Complex p338.||||||05-SEP-14
32152|Harrami Igneous Complex|68553|6|Mentioned|Map legend; schematic diagram.|Early Triassic|Late Permian|Bowen Basin. This unit, as well as the Tandora and Wingfield Suites, the Delubra Gabbro, and various unnamed plutonic units in the Rawbelle Batholith, are all mapped under the symbol, PRgr.||||||
32152|Harrami Igneous Complex|68679|5|Briefly described|p312, p417, p419|Early Triassic|Permian|Rawbelle Batholith, northern New England Orogen. ~80 km2; magnetic images suggest it is more extensive. SiO2-rich samples plot within both the Tandora and Wingfield Suites.||||Steeply abuts Wingfield Greanite. Intrudes Camboon Volcanics.|Biotite monzodiorite and biotite granite; locally mingled with hornblende gabbro. Distinguished by high-K.|
23642|Harry Creek Formation|22800|5|Briefly described|Fig.14 p592|Visean|Visean|||||||
23642|Harry Creek Formation|23032|4|Described|p33,34||Visean|||||||
23642|Harry Creek Formation|23424|4|Described|Table 8.1 p337.||Early Carboniferous|Intruded by Montgomery Range Igneous Complex. Age; Early Carboniferous (Visean)?; superposition and similarities to Lyall Formation. Of Bundock Creek Group, Bundock Basin. Underlies Boroston Fm. Max thickness 560 m.||||||
23642|Harry Creek Formation|23430|5|Briefly described|Plate 14.11||Carboniferous|Also see p507. Of Bundock Creek Group. Graveyard Creek Subprovince.||||||
23642|Harry Creek Formation|23431|5|Briefly described|p541|||||||||
23642|Harry Creek Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Visean|Visean|Of the Bundock Creek Group. Overlies the Boroston Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
23642|Harry Creek Formation|24613|6|Mentioned|p143|||Geological province: Broken River Province, Graveyard Creek Subprovince.||||||07-FEB-11
23642|Harry Creek Formation|24614|5|Briefly described|p191 Fig. 1|||Geological Province: Broken River Province.||||||07-FEB-11
23642|Harry Creek Formation|41260|3|Fully described|p94|||||||||
23642|Harry Creek Formation|41679|6|Mentioned|Fig.2|||||||||
23642|Harry Creek Formation|41739|2|Defined|p305|Visean?||||||||
23642|Harry Creek Formation|41740|6|Mentioned|p222|||||||||
23642|Harry Creek Formation|42054|6|Mentioned|p273|||||||||
23642|Harry Creek Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
23642|Harry Creek Formation|42709|6|Mentioned|map legend|||||||||
23642|Harry Creek Formation|42933|3|Fully described|p172|||Of Bundock Creek Group.||||||25-SEP-06
23642|Harry Creek Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bundock Creek Group.||||||
23642|Harry Creek Formation|43603|5|Briefly described|p9|||||||||
23642|Harry Creek Formation|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Bundock Creek Group. Map symbol (Ch) implies that unit considered entirely Carboniferous.||||||08-MAY-15
23642|Harry Creek Formation|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group. Volcanolithic sandstone, conglomerate and siltstone and tuff; minor coarse-grained sublabile sandstone and conglomerate.||||||17-JUN-13
23642|Harry Creek Formation|67402|4|Described|p239, p245 |Visean|Visean|Bundock Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under alluvial plain and lacustrine conditions. Maximum thickness of 560m. ||||Overlies the Boroston Formation,|Volcanoclastic sandstone, conglomerate, siltstone, tuff and minor sublabile to quartzose sandstone and conglomerate.|
23642|Harry Creek Formation|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Volcanolithic sandstone, conglomerate and siltstone and tuff; minor coarse-grained sublabile sandstone and conglomerate.|
23642|Harry Creek Formation|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Volcanolithic sandstone, conglomerate and siltstone and tuff; minor coarse-grained sublabile sandstone and conglomerate.|
23642|Harry Creek Formation|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Volcanolithic sandstone, conglomerate and siltstone and tuff; minor coarse-grained sublabile sandstone and conglomerate.|
23642|Harry Creek Formation|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably underlain by the Boroston Formation.|Volcaniclastic sandstone, conglomerate and siltstone and tuff; minor coarse-grained sublabile sandstone and conglomerate.|
23642|Harry Creek Formation|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Bundock Basin (Broken River Province).||Bundock Creek Group.||||
23642|Harry Creek Formation|69592|5|Briefly described|p272 Fig.4.61, p273-274, p276|Mississippian|Mississippian|Bundock Basin, Broken River Province. Up to 580m thick. Alluvial plain deposits sourced from the W. No age determined; its stratigraphic context suggests Visean.||Topmost Bundock Creek Group.||Conformably overlies Boroston Formation. Coeval with Lyall Formation.|Mainly fine- to coarse-grained volcaniclastic sandstone interlayered with red siltstone and mudstone; conglomerates with pebbbles and cobbles of acid to intermediate volcanic rocks. Lithic tuffs common in the upper part; thin basal andesite flow.|
23642|Harry Creek Formation|69593|5|Briefly described|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.||Bundock Creek Group.||||
37900|Hawksnest Creek granite|23291|4|Described|p99 Tb. 3.11|Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Described. Geological Province: Georgetown Region.||||||04-MAR-16
70766|Hawthorne Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70766|Hawthorne Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pale pink to pink or pale brown to brown (weathered), fine to medium-grained, uneven-grained to moderately porphyritic, leucocratic biotite granite; commonly partly granophyric; locally with miarolitic cavities.|
70766|Hawthorne Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pale pink to brown, fine- to medium-grained, seriate to moderately porphyritic leucocratic biotite granite; partly granophyric with miarolitic cavities; pegmatitic patches. A-type.|
70766|Hawthorne Granite|73450|6|Mentioned|p8, p16-19, p21|||||||Intruded by John Clifford Road Granite.|I-type granite.|
30697|Hay Mill Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30697|Hay Mill Granite|50536|5|Briefly described|p1.5, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30697|Hay Mill Granite|67323|5|Briefly described|GIS attrib tbl, p12|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Exhibits NW trending linear fabric.||Of Sybella Suite.|||Variably porphyritic medium to coarse biotite granite.|
30697|Hay Mill Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Variably porphyritic medium to coarse biotite granite.|
36251|Hayes Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||25-SEP-06
36251|Hayes Granite|60425|4|Described|p285, p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Included in Brumby Granite in most recent maps. Informally referred to as Nanyeta granite. Fine-grained, granophyric biotite granite. I-type.||||||07-FEB-11
74368|Hazeldene Quartz Diorite|64556|5|Briefly described|p32-36, p56|Late Permian|Late Permian|Age of magmatic emplacement: 268.7+/-1.7Ma. Age analysis details included. Sample analysed was from western region of ROSEDALE - a massive melanocratic porphyritic orthopyroxene-bearing quartz diorite.||||||07-FEB-11
74368|Hazeldene Quartz Diorite|65452|5|Briefly described|p7 Tb.2|Cisuralian|Guadalupian|SHRIMP U-Pb zircon magmatic crystallisation age.|268.7 +/- 1.7 Ma (Carson et al. 2006).||||Orthopyroxene quartz diorite.|
74368|Hazeldene Quartz Diorite|68421|5|Briefly described|Map Legend|Roadian|Wordian|U-Pb zircon dating by Carson et al. (2006).|268.7 +/- 1.7 Ma||||Dark grey, fine to medium-grained, moderately porphyritic orthopyroxene-biotite quartz diorite, with scattered inclusions (to ~10 cm) of biotite gneiss and quartz.|
74368|Hazeldene Quartz Diorite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|268.7 +/- 1.7 Ma (SHRIMP: Carson et al., 2006).||||Orthopyroxene-biotite quartz diorite; scattered inclusions of biotite gneiss and quartz.|
74368|Hazeldene Quartz Diorite|73197|6|Mentioned|p476 Fig.7, p477|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase.|269 or 268 Ma U-Pb||||Mafic intrusives.|
35135|Hazlewood Granite|23042|5|Briefly described|p74,77, Fig 2|||||||||
35135|Hazlewood Granite|60475|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Pink to red, medium grained to slightly porphyritic, granophyric syenogranite.||||||
35135|Hazlewood Granite|61035|4|Described|p10 Tb. 1|Early Carboniferous|Early Carboniferous|Intrudes Mountain View Volcanics and unconformably overlain by Carmila beds. Age: 326.5+/-5Ma (M. Fanning, SHRIMP). Geol Prov: Connors Subprovince. Pink to red, medium-grained to slightly porphyritic, granophyric syenogranite.||||||05-SEP-14
35135|Hazlewood Granite|65388|3|Fully described|p356-357, p90 Fig. 37, p94, 98, 394|Late Carboniferous|Late Carboniferous|Connors Province. New name. Intrudes Mountain View Volcanics. SHRIMP dating inconclusive. But Late Carboniferous age likely. Pink to red, medium-grained to slightly porphyritic granophyric syenogranite.||||||
35135|Hazlewood Granite|68679|5|Briefly described|p363|Mississippian|Mississippian|Southern Connnors Subprovince. Unfoliated.|314.9 +/- 3.9 Ma (SHRIMP: Fanning et al., 2009).|||||
35135|Hazlewood Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|315+/-3.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
23646|Heathfield West Tonalite|22847|3|Fully described|p 50|Early Devonian|Late Silurian|||||||
23646|Heathfield West Tonalite|23422|5|Briefly described|p213 Table 6.8|||||||||
23646|Heathfield West Tonalite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23646|Heathfield West Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 99. I-Type.||||||
23646|Heathfield West Tonalite|24424|5|Briefly described|p526|Silurian|Silurian|Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
23646|Heathfield West Tonalite|42245|2|Defined|p36|Early Devonian|Late Silurian|||||||
23646|Heathfield West Tonalite|42633|5|Briefly described|Table 1 P8|||||||||
23646|Heathfield West Tonalite|42750|6|Mentioned|p43|||||||||
23646|Heathfield West Tonalite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23646|Heathfield West Tonalite|43259|4|Described|Appendix 1,p22.|Early Devonian|Late Silurian|||||||
23646|Heathfield West Tonalite|43933|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23646|Heathfield West Tonalite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23646|Heathfield West Tonalite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23646|Heathfield West Tonalite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23646|Heathfield West Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Heathfield West tonalite.||Unit in Millchester Supersuite.||||
23646|Heathfield West Tonalite|62521|5|Briefly described|p55|||Of Millchester Creek Supersuite. Geological Province: Ravenswood Batholith. See also Heathfield West Granodiorite.||||||14-JAN-08
28602|Hecate Granite|23162|5|Briefly described|p881||Early Cretaceous|Largest Cretaceous pluton in the Connors Arch. Age Zn SHRIMP of 130.8+/-3.4Ma.||||||22-APR-08
28602|Hecate Granite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
28602|Hecate Granite|31984|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
28602|Hecate Granite|32553|4|Described|p56|||||||||
28602|Hecate Granite|32554|6|Mentioned|p17|||||||||
28602|Hecate Granite|32556|4|Described|Table 4|||L.Cret.||||||
28602|Hecate Granite|33202|6|Mentioned|p28|||||||||
28602|Hecate Granite|34975|6|Mentioned|p917|||||||||
28602|Hecate Granite|35266|6|Mentioned|p201|||||||||
28602|Hecate Granite|35467|6|Mentioned|p182|||||||||
28602|Hecate Granite|35872|6|Mentioned|p454|||See also Table 1.||||||
28602|Hecate Granite|36472|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
28602|Hecate Granite|38365|6|Mentioned|p11|||||||||
28602|Hecate Granite|39445|5|Briefly described|Table 12|||||||||
28602|Hecate Granite|41246|6|Mentioned|Map legend|Cretaceous||||||||
28602|Hecate Granite|44815|14|Not recorded|unknown (p313-346)||Cretaceous|||||||
28602|Hecate Granite|45071|6|Mentioned|p87|||Refers Paine et al. (1970)||||||
28602|Hecate Granite|45151|5|Briefly described|Table 12|||See also Table 7.||||||
28602|Hecate Granite|48922|3|Fully described|p56|||||||||
28602|Hecate Granite|64570|6|Mentioned|p855|Early Cretaceous|Early cretaceous|Age: 130.8+/-3.4Ma (SHRIMP).||||||22-DEC-08
28602|Hecate Granite|65706|4|Described|p12; Tb.1 p15,16,18; p27 Fig.5,p34 Fig.7|Early Cretaceous|Early Cretaceous|See also p36-7, p46-7, p53, p55, p56, p58-60, p99, p111, p141. Quartz veins contain Cu mineralisation at Euri Creek; hosts the Julivon Creek porphyry Cu-Mo system; gold and Au-Ag-Cu mineralisation.||||Intrudes Carmila beds, Thunderbolt Granite, Urannah Igneous Complex.|Biotite-hornblende granodiorite, hornblende monzogranite, minor aplitic microgranite, diorite.|
28602|Hecate Granite|68358|5|Briefly described|p6, p8, p19|Early Cretaceous|Early Cretaceous|Adjacent to the Hillsborough Basin. High U-Th-K radiometric responses.|||||Granodiorite and adamellite, with late-stage leucocratic phases, and an aplitic microgranite.|05-MAR-19
28602|Hecate Granite|68901|5|Briefly described|p50|||Occurs near the Pretty Bend Quartz Monzodiorite.|131 +/- 3 Ma (Allen et al, 1998)||||Mainly massive, unfoliated granite.|26-SEP-18
28602|Hecate Granite|69594|4|Described|p566-568, p569 Fig.7.43, p571 Fig.7.46|Cretaceous|Cretaceous|Bowen region. A large (~725 km2) normally-zoned pluton. Generally deeply weathered, but locally forms very prominent outcrops. Several photographs. Geochemistry plot.|130.8 +/- 3.4 Ma (SHRIMP: Allen et al. 1998).|||Is intruded by Roma Peak Granite.|(Clinopyroxene-)biotite-hornblende quartz monzodiorite to biotite monzogranite; granodiorite is the most common rock type. Commonly contains prominent hornblende laths, conspicuous titanite euhedra, pink or white K-feldspar, and traces of allanite.|
28602|Hecate Granite|70673|5|Briefly described|p8, p118, p128|Early Cretaceous|Early Cretaceous|Forms prominent outcrops. Part of a major magmatic event. within uncertainty of the Hecate Granite and Alick Creek Tonalite.|130.8 +/- 3.4 Ma (Allen et al., 1998).|||||
28602|Hecate Granite|71592|5|Briefly described|Appendix A.||||131+/-3.4 Ma (SHRIMP U-Pb zircon).||||Granodiorite.|
28602|Hecate Granite|73036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Five subunits recognised, with distinct descriptions (two geophysical only). Geophysical units mainly characterised by radiometric response: White tones on ternary radiometric image; Mainly mottled mauve tones on ternary radiometric images and low to moderate response on aeromagnetic images.|||||Pale pink, or pale pinkish grey to pale grey, medium-grained, uneven-grained hornblende-biotite (minor) and biotite-hornblende granodiorite to quartz monzodiorite; some porphyritic and containing minor titanate, allanite.  See also comments.|
36588|Hecta microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 338.  I-Type.||||||
77874|Hedleys Sandstone|67323|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Variation on Hedleys Sandstone Member. Detrital [?zircon] ages: 1591+/-10 Ma (2000), 1577 +/-29 Ma (Magee et al, in prep).||Implied to be of South Nicholson Group.||||
77874|Hedleys Sandstone|67539|5|Briefly described|p14|||North of the Elizabeth Creek fault. Raised to formation rank.||Of the South Nicholson Group.||Overlain by the Pandanus Siltstone.||
77874|Hedleys Sandstone|68146|5|Briefly described|p21-23, p29, p196-197|||Geochronology by Magee et al. (in press). This value was applied in determining a constraint on the MDA of Burangoo Sandstone in the current study.|1577 +/- 29 Ma; maximum depositional age.|Basal Wild Cow Subgroup.||||
77874|Hedleys Sandstone|68575|4|Described|p3,p6-7,p10-17,p19,p21,p125,p128,p134|||South Nicholson Basin. Shows significantly different provenance from that of Burangoo Sandstone.|1602 +/- 22 Ma (maximum depositional age).|Basal South Nicholson Group.||Unconformably overlies Doomadgee Formation.|Cross-bedded, sublithic to lithic, fine- to very coarse-grained and granule sandstone, interbedded with lenses of pebble to cobble conglomerate.|
77874|Hedleys Sandstone|69591|4|Described|p52-54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Appears as Hedley Sandstone in Fig.2.47. Predominantly fluvial. 1577 Ma age by Magee et al. (in press).|1591 +/- 10 Ma; 1577 +/- 29 Ma (MDA).|Wild Cow Subgroup.||Is overlain by Pandanus Formation.|Cross-bedded, medium- to coarse-grained quartzose sandstone with scattered granule and pebble bands; pebble to cobble conglomerate basal lenses with well-rounded quartz and quartzite and subangular-subrounded stromatolitic and oolitic chert clasts.|
77874|Hedleys Sandstone|71369|3|Fully described|p1, p6, p8-15, p19, p47, p49|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Raised to Formation status in this study (Sweet, 2017); previously Hedleys Sandstone Member (Rawlings et al., 2008) of Constance Sandstone. 35m thick in the type section from 198870E 8025500N to 199120E 8025290N in HEDLEYS CREEK sheet (diagram); slight variation of coordinates from the original by Rawlings et al. (2008). Outcrop pattern indicates left lateral (fault) movement of 700-800m.|c.1500 Ma.|Wild Cow Subgroup.||Unconformably overlies Doomadgee Formation and Widdallion Sandstone Member (Lawn Hill Formation). Is overlain by Pandanus Formation.|Basal conglomerate and very thick-bedded conglomeratic sandstone, gradually fining-up into thick-bedded, medium- to coarse-grained, strongly cross-bedded sandstone.|20-FEB-18
77874|Hedleys Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1602+/-22 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
77874|Hedleys Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Pandanus Sandstone.|Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Pandanus Sandstone.|Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|19-MAR-20
77874|Hedleys Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|10-DEC-19
77874|Hedleys Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|10-DEC-19
77874|Hedleys Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|
77874|Hedleys Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.|||||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|
77874|Hedleys Sandstone|72526|5|Briefly described|p8 Fig.1.3|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||?Wild Cow Subgroup, South Nicholson Group||Shown as  overlying Lawn Hill Formation and underlies Pandanus Formation.||
77874|Hedleys Sandstone|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin. Shown as overlying MacNamara Group in NT and QLD.||Wildcow Subgroup||Underlies Pandanus Formation.|Includes sandstone.|
77874|Hedleys Sandstone|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson.||Wildcow Subgroup||Underlies Pandanus Formation.|Includes sandstone.|
77874|Hedleys Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in QLD. Distinct from Hedleys Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77874|Hedleys Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. Overlain by Pandanus Formation.||Wildcow Subgroup?, South Nicholson Group||Partly underlain by Widdallion Sandstone Member unconformably. Partly underlain(?) by Lawn Hill Formation.||
77874|Hedleys Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Overlain by Pandanus Formation.||
68999|Hefferon Creek Gabbro|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Pyroxene-hornblende gabbro with common pegmatite, aplite and microgranite dykes.||||||
68999|Hefferon Creek Gabbro|65388|2|Defined|p319-320,  p301 Fig 98, p303, 304, 340|Early Triassic|Late Permian|Previously unmapped unit.  Likely to intrude surrounding Colodon Granodiorite, but contacts masked by soil cover. Dark green, medium to coarse-grained, hornblende-clinopyroxene gabbro. Generally very poor outcrop.||||||
68999|Hefferon Creek Gabbro|68679|5|Briefly described|p418-419|||Rawbelle Batholith. Circular pluton ~2.5km diameter; distinct magnetic high.||||Is enclosed by (probably intrudes) Colodon Granodiorite.|Pyroxene-hornblende gabbro.|
36560|Heidelberg complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 228.  I-Type.||||||
23647|Heneage Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23647|Heneage Granite|22781|4|Described|p32|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
23647|Heneage Granite|23420|4|Described|p 149 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Burns Granite||||||
23647|Heneage Granite|42610|2|Defined|p14|Early Devonian|Early Devonian|Age assumed approx. 400Ma. Included in "Kintore Adamellite" of B135.||||||
23647|Heneage Granite|43738|6|Mentioned|Fig.12,p38|||||||||
23647|Heneage Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
23647|Heneage Granite|71849|5|Briefly described|p8, p195|Devonian|Devonian|||Ebagoola Suite.||||
23647|Heneage Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.||Grades into Burns Granite.|Pale grey to buff or cream porphyritic muscovite-biotite granite; phenocrysts of K-feldspar typically 2-3 x 1 cm.|
41790|Herbert Creek beds|60479|5|Briefly described|Map Legend|Tertiary|Tertiary|Lacustrine mudstone, shale, oil shale, sandstone, lignite.||||||
41790|Herbert Creek beds|60481|5|Briefly described|Map Legend|Tertiary|Tertiary|Lacustrine mudstone, shale, oil shale, sandstone, lignite.||||||
41790|Herbert Creek beds|61035|5|Briefly described|p19, p21|Tertiary|Tertiary|Informal name. Thickness: 1300m.  Geological Province: Herbert Creek Basin. Consists of mudstone, sandy, micaceous shale and subordinate semifriable lithic sandstone and pebble conglomerate; severla intervals of oil shale are present.||||||07-FEB-11
41790|Herbert Creek beds|65388|5|Briefly described|p226-227|Tertiary|Tertiary|Herbert Creek Basin rocks are herein assigned to the Herbert Creek beds, consisting mainly of mudstone, sandy, micaceous shale and subordinate semi-friable lithic sandstone and pebble conglomerate; several intervals of oil shale. 800-1300m thick. Mostly identified from drilling. Overlies Pyri Pyri Granite?||||||
41790|Herbert Creek beds|69599|5|Briefly described|p586, p589|Eocene|Eocene|Herbert Creek Basin. >800m (possibly up to 1300m) thick. Poor outcrop; only a few deeply weathered exposures. Contains several economic oil shale blocks, but no development has occurred. RELATED UNITS (continued): Also correlated (at least partly) with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek and Rossmoya beds; Flinders Dolomite; see COMMENTS for more.|Mudstone, sandy shale, lithic sandstone, pebble conglomerate and subordinate oil shale.|
36177|Herberton Hill Granite|23506|5|Briefly described|Map Legend||Early Permian|of O'Briens Creek Supersuite.||||||
36177|Herberton Hill Granite|60425|4|Described|p45 Tb. 3, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Cherry Tree Suite (O'Briens Creek Supersuite).Unconformable below/or intruded by Slaughter Yard Ck VolcsDetailed lith.included; I-type.Delineated as discrete unit by Clarke (1990, 1995); incl.in Saint Patrick Hill Granite (Donchak and Bultitude 1998)||||||07-FEB-11
36177|Herberton Hill Granite|69593|6|Mentioned|p486||||322.2 +/- 4.4 Ma (Murgulov, 2006).|||||
29979|Herberton Suite|23291|5|Briefly described|p96 Tb. 3.11|Late Carboniferous|Late Carboniferous|Parent: O'Brien's [misspelling of O'Briens] Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
29979|Herberton Suite|23616|5|Briefly described|p75|||Of O'Briens Creek Supersuite.||||||
29979|Herberton Suite|43060|6|Mentioned|p101|||of O'Briens Creek Supersuite||||||
29979|Herberton Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of O'Briens Creek Supersuite.||||||15-JUN-06
29979|Herberton Suite|60425|5|Briefly described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Includes Atlanta, Hales Siding, Jumna and Lass O'Gowrie Granites. Ages range from ~314-~303Ma (Rb-Sr). I-type.||||||07-FEB-11
36582|Hermit granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 330  I-Type.||||||
36582|Hermit granodiorite|60425|5|Briefly described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Informal name. Part of Ootann Supersuite. I-type. Grey, medium-grained hornblende-biotite granodiorite.||||||07-FEB-11
80783|Hero Formation|67323|5|Briefly described|GIS attrib tbl, p13|Paleoproterozoic|Paleoproterozoic|Isa Superbasin. Mass-flow dominated sediments.||Mount Isa Group. Informally subdivided into 7 units.||Time equivalent to Moondarra Formation.|Matrix-supported volcanilithic breccia and conglomerate. Fine-grained, greenish, pebbly wacke. Pebbly conglomeratic sandstone. Coarse to fine-grained heterolithic sandstone, siltstone and shale.|
80783|Hero Formation|69591|5|Briefly described|p55|||Leichhardt River Domain, Isa Superbasin. Part of Gun Supersequence. Alluvial fan and delta fan deposits.||Mount Isa Group.|||Matrix-supported volcanilithic breccia and conglomerate, subordinate poorly-sorted lithic and feldspathic sandstone, minor siltstone.|
80783|Hero Formation|71960|4|Described|p85-101, 102-104, 106, 82, 83 Fig.6,p84|Proterozoic|Proterozoic|In Hero Fault Zone area. Previously included in the Warina Park Quartzite, but sedimentologically different and not directly connected. Type section shown Fig. 9 p88. location base: 6757 355411, top: 6757 357412 [AGD 66 assumed]. 212 m thick in type section. See Facies A-F p89-101. Depositional environment: alluvial fan delta.||Of Mount Isa Group. ||Lateral equivalent of  Warrina Park Quartzite? Lateral and upward gradational transitions with Moondarra Siltstone.|Immature ferruginous clastics. Conglomerate, volcaniclastic breccia and minor sandstone in type section.|
80783|Hero Formation|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Hero Fault Zone. Fan delta. ||Of Mount Isa Group|||Mass-flow dominated conglomerate, breccia; stream flow conglomerate; fine-grained pabbly wacke; pebbly sandstone; conglomeratic sandstone; coarse heterolithic conglomerate, sandstone, shale; fine-grained sandstone, siltstone, shale.|
73904|Herries Suite|63748|5|Briefly described|p33|Late Permian|Early Permian|Of Herries Supersuite. Includes the Herries, Palgrave and Fairleigh Granites.||||||07-FEB-11
73904|Herries Suite|68679|5|Briefly described|p456, p458, p460-461, p464-465|Permian|Permian|Northern New England Batholith. ~158 km2. Late Permian. Geochemistry discussed; photographs, geochemical plots.||Stanthorpe Supersuite.|Herries, Palgrave, Fairleigh Granites.||Medium- to high-K granites, distinguished by absence of felsic, highly fractionated rocks; almost complete absence of associated mineralisation; abundant mafic minerals; widespread hornblende; common mafic enclaves; absence of miarolitic enclaves.|
73904|Herries Suite|71628|5|Briefly described|p19: 60, 65-66, 68, 71|||Redefined in this study. Previously comprised the Herries, Palgrave and Fairleigh Granites.||Herries Supersuite.|Herries, Palgrave, Clare Hills and Fairleigh Monzogranites.|||
73827|Herries Supersuite|63748|5|Briefly described|p32-33, p34|Late Permian|Early Permian|Includes the Herries, Clare Hills, Maryland Suites. Geochemistry included (p34). See also p27 Fig.27.||||||07-FEB-11
73827|Herries Supersuite|68111|5|Briefly described|p968 Tb.1||||||Includes Palgrave Granite, Fairleigh Granite, Clare Hills Granite, and Herries Granite.|||
73827|Herries Supersuite|69639|5|Briefly described|p1, p44, p74, p151, p217, p220, p222|Permian|Permian|New England Orogen.|||Includes the Maryland Suite, Clare Hills Granite, Fairleigh Granite, Herries Granite, Boonoo Granite, Palgrave Granite and the Four Bull Granodiorite.|||
73827|Herries Supersuite|70876|4|Described|p2, p58, p79-p80|Late Permian|Late Permian|New England Orogen. Consists entirely of strongly evolved I-type granites that are characterised by their lack of mineralisation (relative to the Stanthorpe Granite), geochemistry, common mafic enclaves and lack of miarolitic cavities. Donchak et al, (2013) incorporated the Herries Supersuite (in addition to the Bullaganang, Ballandean and Mount You You Supersuites into the Stanthorpe Supersuite despite the great age range of all these Supersuites. In light of new dates and previous dates for the aforementioned supersuites this volume suggests revisiting the definition of the Stanthorpe Supersuite.|||Includes the Newton Boyd Granodiorite, Botumburra Range Monzogranite, Boonoo Granite and the Palgrave Granite.|||
73827|Herries Supersuite|71628|6|Mentioned|p19: 21, 60, 63, 65, 68, 71, 98-99||||||Clare Hills, Herries Suites.|||
80775|Hidden Glen Monzogranite|68679|5|Briefly described|p420-421|Late Triassic|Late Triassic|Gayndah-Gladstone belt.|||||Biotite monzogranite.|
79370|Hidden Valley Rhyolite|70740|4|Described|i, iv, p8, p82 fig 50, p84-p86|Carboniferous|Carboniferous|Drummond Basin. SHRIMP age derived from Black (1994). Name derived from the Old Hidden Valley Station. Interpreted thickness ranging from 150 to 200m. A new type locality is nominated and the outcrop characteristics and its lithology here is very briefly mentioned. May also overlie the Star of Hope Formation and the Ukalunda Formation. Previously mapped as Locharwood Rhyolite but exhibits significant geochemical differences and on that basis has been reinterpreted as a separate unit. Also intruded by Charlie Creek Microgranite, unconformably overlies Bimurra Volcanics, and overlies Pyramid Rhyolite. Overlain by unnamed Bulgonunna Volcanic Group units, probably faulted against the Star of Hope Formation. Distribution is discussed. See also p88, p99-p100, p102-p106, p121, p122.|304.7 +/- 4 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Intruded by the House and Kitchen Granite and the Billy-Can Creek Granite. Overlies the Collins Creek Rhyolite. Faulted against the Ukalunda Formation and Sunbeam Granodiorite.|Massive and very extensive, moderately crystal-rich and strongly welded rhyolitic ignimbrite characterised by strongly embayed quartz and a pale grey ash-rich matrix.|
79121|Highbury Basalt|70913|3|Fully described|p58-p60, p1, p8 fig 3, p11, p44, 45|Permian|Late Carboniferous|Gympie Province. New name restricted to the lowermost volcanic unit in the succession. In part replacing Highbury Volcanics. Named for Highbury Hill, Chatsworth. More amygdaloidal than Mary Basalt. A type section is mentioned in addition to a reference drill hole. In excess of 300m thick; though total thickness is unknown.  Base of unit not penetrated. See also p67, p77, App 1 maps, Highbury Formation p58.|Max dep age 302 Ma detrital Zr.|Gympie Group||Overlain by the Excelsior Conglomerate Marker Bed of Dawn Formation.|Basalt lavas, flow and tuff breccias, hematitic, scoriaceous and pyroxene phyric.|18-SEP-17
79121|Highbury Basalt|73303|6|Mentioned|p61 Fig.2, p62, p65 Fig.5|Cisuralian|Cisuralian|New England Orogen. Gympie Terrane, southern. Contains evidence of subaqueous deposition. Considered to be the same lithological unit as the Mant Basalt.||||Underlies Dawn Formation.|Basaltic unit.|
79750|Highlanders Bonnet Granodiorite|70673|6|Mentioned|p118|Early Cretaceous|Early Cretaceous|Forms prominent outcrops.||||||
79750|Highlanders Bonnet Granodiorite|73029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||White to very pale pink or pale pinkish grey, medium-grained, moderately porphyritic hornblende-biotite granodiorite; with traces of titanite and scattered mafic inclusions to c. 35 cm (most < 10 cm); locally miarolitic.|
40859|Highway Metavolcanics|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Of the Balcooma Metavolcanic Group.  Laminated to thickly bedded siliceous, volcanic meta-siltstone and meta-arenite.||||||
40859|Highway Metavolcanics|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.||Unit in Balcooma Metavolcanic Group.|||Laminated to thickly bedded siliceous, volcanic meta-siltstone and meta-arenite.|
40859|Highway Metavolcanics|68731|6|Mentioned|p152, p154|Early Ordovician|Early Ordovician|Age constrained by the parent Balcooma Metavolcanic Group.||Of the Balcooma Metavolcanic Group.|||Comprises well-bedded or laminated pyritic siliceous siltstone or metatuff and minor metarhyolite.|
78931|Hildura Quartz Monzodiorite|65388|4|Described|p258-259, p261, 236, 237, 238, 319|Early Permian|Late Carboniferous|Previously Hildura Granodiorite. Relationships with other units uncertain. Tentative age assigned. White to grey, medium grained quartz monzodiorite in type section. Heterogeneous, with quartz monzonite, quartz monzodiorite and granodiorite dominant in places with local granite and gabbro.||||||
78931|Hildura Quartz Monzodiorite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Relationships with surrounding units uncertain. Age tentative.|||||Includes medium-grained hornblende-biotite granodiorite or quartz monzodiorite, quartz monzonite, and granodiorite with local granite and gabbro.|
82115|Hillside Bore Granite|73553|4|Described|p8 Fig.1.2.3, p200-205|Calymmian|Calymmian|Mary Kathleen Domain, northern. Williams-Naraku Igneous Province. New unit. Described as unnamed unit Plg/k in most recent digital coverage (GSQ, 2018), depicted as a group of irregularly shaped bodies. Name derived from a water bore adjacent to an outcrop on Boomarra Station. High-level intrusion occurring as pods and dykes/veins intruding the Corella Formation. Crops out at the northern end of the Boomarra Horst, occurs as large but isolated bouldery outcrops. Difficult to distinguish based on geoophysical characteristics.|1500+/-6 Ma U-Pb SHRIMP (Bodorkos et al., 2020)|||Intrudes Corella Formation, Boomarra Metamorphics|Magnetic, fine-grained, even-grained, leucocratic biotite monzogranite to syenogranite; variations include a weakly porphyritic phase, local graphic textures, local strong foliation, pegmatite.|
36433|Hinchinbrook Granite|23423|4|Described|p313 Table 7.4||Early Permian|Part of the Ingham Batholith. Age: 275 +/- 5 Ma (Rb-Sr). A-type granite.  See also p254-255.||||||
36433|Hinchinbrook Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 160.||||||
36433|Hinchinbrook Granite|23617|4|Described|Table 2 p16||Early Permian|Age: 275 Ma (Rb-Sr). Previously referred to as Hinchinbrook granite (informal). A-Type granite. Intrudes felsic rock assigned to Wallaman Falls Volcanics. Also Table 3 p52. Kennedy Province. Also see p32.||||||16-APR-09
36433|Hinchinbrook Granite|23618|5|Briefly described|map legend||Early Permian|||||||
36433|Hinchinbrook Granite|60425|3|Fully described|p53, p58-9 Tb. 4, p105-107|Early Permian|Early Permian|Of Hinchinbrook Supersuite and Ingham Batholith. Age: 275+/-5Mas (Rb-Sr). A-type, mainly (arfvedsonite-)biotite granite with numerous interstitial and miarolitic cavities; minor porphyritic microgranite, pegmatite, aplite, pyroxene-bearing granite.||||||07-FEB-11
36433|Hinchinbrook Granite|69593|5|Briefly described|p492, p494, p496|Permian|Permian|Paluma Subprovince, Kennedy Igneous Association. Forms prominent outcrops on Hinchinbrook Island.|~275 Ma (Stephenson et al., 1990).||||A-type. (Arfvedsonite-)biotite leucogranite, minor microgranite. Traces of fayalite locally. Commonly horizontally layered; arfvedsonite crystallised late, common in miarolitic cavities.|
36433|Hinchinbrook Granite|73450|4|Described|p103-105|Permian|Carboniferous|Crops out as an elongate, tabular, N-NW-aligned pluton making up most of Hinchinbrook Island east of Cardwell; forms rugged, mountainous country. Described as mainly hypersolvus and vuggy or drusy to varying degrees, and features sporadic subhorizontal layering and downward facing solidification textures.|||||Fine- to medium-grained, leucocratic, arfvedsonite-biotite alkali feldspar granite.|
75115|Hinchinbrook Supersuite|60425|3|Fully described|p58 Tb. 4|Early Permian|Early Permian|Contains Hinchinbrook Granite. Age: 275+/-5Mas (Rb-Sr). A-type - see Hinghinbrook Granite for detailed lithology. Part of the Ingham Batholith in the Ravenshoe-Ingham Belt together with Ingham Supersuite.||||||07-FEB-11
33425|Hivesville Granite|23799|3|Fully described|p74, p14 Tb. 1|Permian|Permian|Northern section previously mapped as Wigton Adamellite; southern section as part of Boondooma Igneous Complex (Murphy and others, 1976). Overlain by Main Range Volcanics.  Geological Province: Yarraman Subprovince. See also p115 Fig. 10.||||||
33425|Hivesville Granite|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
33425|Hivesville Granite|60371|5|Briefly described|Map Legend|Triassic|Permian|Biotite (-hornblende) granite; locally intruded by or intermixed with numerous small microdiorite bodies.||||||
33425|Hivesville Granite|68679|5|Briefly described|p323, p410, p414-416, p420|||West of the Esk Basin, northern New England Orogen. Formerly mapped as part of Wigton Granite (Ellis, 1968).  Proximity to this unit (and other named units) increases the metamorphic grade of rocks in the Fifer Creek Metamorphics. Has lower Na2O and K2O and higher CaO. Geochemical plot. Several ages given within this range.|274 +/- 28 Ma to 250.1 Ma.||||Coarsely megacrystic biotite granite with characteristic rapakivi texture.|
24311|Hobble Creek Member|40247|5|Briefly described|p208|||||||||
24311|Hobble Creek Member|40954|6|Mentioned|p133|||||||||
24311|Hobble Creek Member|42975|6|Mentioned|Fig.2 p257|||of Lowmead Formation||||||
24311|Hobble Creek Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably overlain by the Harpur Creek Member.|Dominantly sandstone with interbedded claystone; red, yellow and green mottling in part.|
24311|Hobble Creek Member|68421|5|Briefly described|Map Legend|Eocene|Eocene|Lowmead Graben.||Of the Lowmead Formation.||Conformably overlain by the Harpur Creek Member.|Dominantly sandstone with interbedded claystone; red, yellow and green mottling in part.|
24311|Hobble Creek Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. 2.3-40m thick; average 20.5m.||Lowmead Formation.||Is overlain by Harpur Creek Member.|Claystone; red and some yellow and green mottling; sporadically sandy and silty.|
35064|Hodgon Granodiorite|23049|3|Fully described|p37|Early Devonian|Late Silurian|Age: 414+/-5Ma. Of the Hodgon Suite.||||||14-APR-08
35064|Hodgon Granodiorite|23283|2|Defined|p22|Devonian|Silurian|||||||
35064|Hodgon Granodiorite|23422|4|Described|p177, p216 Table 6.10|Late Silurian|Late Silurian|Of Hodgon Suite.||||||
35064|Hodgon Granodiorite|23430|5|Briefly described|Table 14.2 p460.||Silurian|Zircon crystallisation 414 +/- 5 Ma. Lolworth Batholith Province||||||
35064|Hodgon Granodiorite|23505|5|Briefly described|Map legend|Devonian|Silurian|Of Amarra Supersuite.||||||14-APR-08
35064|Hodgon Granodiorite|69592|5|Briefly described|p293|Late Silurian|Late Silurian|Lolworth Batholith, Charters Towers Province.|414 +/- 5 Ma (SHRIMP U -Pb zircon).|Hodgon Suite.||||
35062|Hodgon Suite|23049|4|Described|p36|||||||||
35062|Hodgon Suite|23283|4|Described|p22|Devonian|Silurian|||||||
35062|Hodgon Suite|23422|4|Described|p177, p216 Table 6.10|Late Silurian|Late Silurian|||||||
35062|Hodgon Suite|23508|5|Briefly described|Map Legend|Devonian|Silurian|||||||
35062|Hodgon Suite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester, Toms Hole and Upland Supersuites; the Broughton River, Grasstree and Amarra Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
35062|Hodgon Suite|69592|4|Described|p292|Late Silurian|Late Silurian|Lolworth Batholith, Charters Towers Province. Geochemical plots.|c.414 Ma.||Hodgon Granodiorite.|Intrudes Cape River Metamorphics.|Hornblende-biotite granodiorite and granite.|
25061|Hogback Granite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
25061|Hogback Granite|39505|6|Mentioned|p178|||||||||
25061|Hogback Granite|40475|6|Mentioned|Table 2|||||||||
25061|Hogback Granite|41738|6|Mentioned|p168|||||||||
25061|Hogback Granite|41778|2|Defined|Table 2|Late Triassic||See also p375.||||||09-NOV-15
25061|Hogback Granite|42054|6|Mentioned|p273|||||||||
25061|Hogback Granite|43008|5|Briefly described|map legend|||||||||
25061|Hogback Granite|63821|4|Described|p21, p32|Late Triassic|Late Triassic|See also Hogback Granodiorite(prob.misnamed). Age:228+/4Ma (K-Ar biotite). Hornbl.-biotite granite to biotite granite+granophyric aplite. Intrudes undiv.Curtis I.Group, Good Night beds,Goyan Andesite, Mt Marcella Volcs, Wonbah+Moolboolaman Granodiorites.||||||07-FEB-11
25061|Hogback Granite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
25061|Hogback Granite|68679|5|Briefly described|p428, p430-431|Late Triassic|Late Triassic|Cranfield and Murray (1989). Northern New England Orogen. Appears (just) as Hogbac Granite on p428. This age determination contradicts interpretations that this unit intrudes the (younger) Wonbah and Moolboolaman Granodiorites.|228 +/- 4 Ma (K-Ar: Cranfield and Murray, 1989).||||Medium-grained biotite-hornblende granite and granophyre.|
25061|Hogback Granite|73450|4|Described|p24-25|Norian|Carnian|[Also written as 'Hogback Granite' to indicate specific usage]. Included as part of the Hogback Tonalite of Ellis (1968), which was subsequently subdivided into several discrete units by Cranfield and Murray (1989). Exposed over an irregular area southwest of Gin Gin; forms rough, well-forested, extensively dissected, hilly to mountainous country (Hogback Range). Yielded a K-Ar biotite age of 228 +/- 4 Ma (Cranfield and Murray, 1989). Interpreted to be a high-level, postorogenic intrusion possibly related to the Arangbanga Volcanic Group (Ellis, 1968; Cranfield, 1994).|228 +/- 4 Ma K-Ar|||Intrudes Curtis Island Group, Good Night beds, Goyan Andesite, Mount Marcella Volcanics, Aranbanga Volcanic Group, and the Wonbah, Briggs and Moolboolaman granodiorites.|Pink, leucocratic, medium- to locally coarse-grained granite consisting predominantly of quartz, K-feldspar, plagioclase, biotite and opaques.|
73533|Hogsflesh Creek Suite|62521|5|Briefly described|p25, p26|||Of the Hogsflesh Creek Supersuite. Geological Province: Ravenswood Batholith. Includes Hogsflesh Creek Granodiorite.||||||14-JAN-08
38173|Hogsflesh Creek Supersuite|23422|4|Described|p171|||See also Hogsflesh Supersuite.||||||
38173|Hogsflesh Creek Supersuite|62521|4|Described|p1, p25, p26|Middle Ordovician|Early Ordovician|Comprises: Hogsflesh Creek Granodiorite and Suite, and Towers Hill and Chipley Granites +  unnamed granites. Geological Province: Ravenswood Batholith.||||||21-DEC-07
38173|Hogsflesh Creek Supersuite|68731|5|Briefly described|p148, p149, p150|Middle Ordovician|Early Ordovician|Hutton and Crouch (1993); Hutton et al. (1994); Hutton and Rienks (1997). Previously included the Chipley Granite by Hutton and Crouch (1993, 1993), but Hutton et al. (1994, 1994) separated it out on the basis of geochemistry.|||||Comprises mainly grey to greyish pink biotite and hornblende-biotite granite to granodiorite.|13-MAY-16
25063|Holroyd Group|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||12-JAN-05
25063|Holroyd Group|22781|3|Fully described|p17|Proterozoic|Proterozoic|Savannah Province||||||
25063|Holroyd Group|22811|4|Described|p597, Fig.2 p598|Mesoproterozoic|Mesoproterozoic|of Savannah Province||||||
25063|Holroyd Group|23420|4|Described|p 143 table 4.4||Mesoproterozoic|Age: <1560+/-13Ma, >1430+/-10Ma. Faulted against Edward River Metamorphic Group. Consists of all rocks previously assigned to the Holroyd Matamorphics, except those along the western egde. In the Savannah Province||||||
25063|Holroyd Group|23425|5|Briefly described|p370.|||||||||
25063|Holroyd Group|23430|4|Described|p454-455|||Savannah Province.||||||
25063|Holroyd Group|23431|5|Briefly described|p535|||||||||
25063|Holroyd Group|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|||||||
25063|Holroyd Group|42610|6|Mentioned|p4|||Variation on Holroyd Metamorphics & Holroyd Metamorphic Group.||||||
25063|Holroyd Group|42640|5|Briefly described|p9|||||||||
25063|Holroyd Group|42650|6|Mentioned|p13|||Redefinition of Holroyd Metamorphics in Ebagoola area||||||
25063|Holroyd Group|43287|6|Mentioned|Map Legend||Paleozoic|||||||07-NOV-08
25063|Holroyd Group|43596|3|Fully described|p6 Fig. 6, p17, p1929 Tb. 1||Mesoproterozoic|Part of Savannah Province, together with Coen, Edward River and Staaten Metamorphic Groups. Formerly known as Holroyd Metamorphics. Comprises 9 named units. Max. thickness: 10km.||||||15-JAN-09
25063|Holroyd Group|43665|4|Described|p10||Proterozoic|||||||
25063|Holroyd Group|43730|6|Mentioned|p13|||||||||
25063|Holroyd Group|43820|5|Briefly described|Map Legend||Mesoproterozoic|||||||
25063|Holroyd Group|63866|4|Described|p76, p80-p81, p85|||Savannah Subprovince, Coen Region. Crops out along the western side of the Coen Region and is faulted to the west by the Cattle Swamp Shear Zone. Up to 10km thick and consists of ten mappable units (most unnamed in this study). Dates interpreted from grains of a phyllite in this group includes c. 1593, c. 1639, c. 1696 Ma and c. 1746 although due to the small size of the grains the relevance of these ages is uncertain.|||Includes the Astrea Formation and the Strathburn Formation.||Medium-grained clastic sediments.|
25063|Holroyd Group|69591|5|Briefly described|p76-80, p111|||Coen Inlier, Savannah Province. Comprises 13 formations (including 10 mappable units) totalling about 10km of basin fill. Crops out over c.4500 km2. Consists of all the rocks previously assigned to the Holroyd Metamorphics except for those along the western edge of the Inlier (that are now the Edward River Metamorphic Group). Appears as Holyoyd [sic] Metamorphic Group on p74 Fig.2.71. Is extensively intruded by the Cape York Peninsula Batholith. Has undergone six regional deformation events.|~1560 Ma (MDA: Neumann and Fraser, 2007).||Coleman River Gneiss; Dinah, Astrea, Newirie, Strathburn and Strathmay Formations; Sugarbag Creek, Carysfort and Gorge Quartzites; Carew Greenstone.||Variably deformed and metamorphosed metasiltstone/sandstone, slate, phyllite, quartzite, schist, gneiss, metadolerite (greenstone) and amphibolite.|
25063|Holroyd Group|70822|5|Briefly described|p112|||Savannah Province.|c.1600 Ma.||||Mafic magmas.|
25063|Holroyd Group|71792|5|Briefly described|p3, p5, p8|Mesoproterozoic|Paleoproterozoic|Savannah Province. A magmatic crystallisation age of 1460 Ma is provided. Appears truncated in magnetic data.|1616 and 1560 Ma (Max. deposition ages)|||||
25063|Holroyd Group|71849|5|Briefly described|p8, p195|Mesoproterozoic|Mesoproterozoic||||Strathburn Formation.|||
25063|Holroyd Group|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||||Strathmay Formation, Strathburn Formation, Gorge Quartzite.|||
25063|Holroyd Group|72983|6|Mentioned|p6, p83|||New work led to a mapped outcrop of this unit being reassigned to the Lochs Gneiss.||||||
25063|Holroyd Group|73083|6|Mentioned|p59|||||||||
25063|Holroyd Group|73387|6|Mentioned|p1, p37||||||Strathburn Formation|||19-DEC-22
23651|Hope Vale Granite|23511|5|Briefly described|Map Legend||Early Permian|||||||
23651|Hope Vale Granite|42369|3|Fully described|p53|Early Permian||Previously mapped as Findlayson Granite. Similar to Puckley Granite which dates 276+/- 3Ma Rb-Sr.||||||
23651|Hope Vale Granite|42474|5|Briefly described|p27|||||||||
23651|Hope Vale Granite|43070|2|Defined|p3|Early Permian||||||||
23651|Hope Vale Granite|50587|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Yates Supersuite. Geological Province: Kennedy Province. Biotite granite.  Fine to medium grained.||||||28-JUN-04
23651|Hope Vale Granite|60425|5|Briefly described|p54 Tb. 4, p272-3 Appdx. 1|Late Permian|Permian|Of Hope Vale Suite (Yates S'suite). Age probably Late? Permian.I-type. Slightly to mod'ly porph, med.gr. (hornblende-)-biotite granite + accessory allanite, zircon, apatite, ilmenite; scattered mafic enclaves common - more lithological details included.||||||07-FEB-11
23651|Hope Vale Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Yates Supersuite.||||
23651|Hope Vale Granite|72983|4|Described|p1, p3, p7, p19, p35-40|Kungurian|Kungurian|Kennedy Igneous Association. Cape York region. Northern-most unit of the Yates Supersuite. Similar age and lithology to the Puckley Granite. Suspected coeval with Collins Weir Rhyolite, Tinaroo Granite, Featherbed Volcanic Group and Nychum Volcanics.|280.4 +/- 1.6 Ma SHRIMP U-Pb|Yates Supersuite||Intrudes Hodgkinson Formation. Overlain by Dalrymple Sandstone and Piebald Basalt.|Includes massive, fine- to medium-grained, moderately porphyritic hornblende-biotite granite with diorite and metasedimentary inclusions.|
69331|Hope Vale Suite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Permian|Of Yates Supersuite. Includes Hope Vale Granite. Age is probably Late? Permian. I-type.||||||07-FEB-11
36370|Horn Island Granite|23421|4|Described|Tb 5.3 p164|Early Permian|Late Carboniferous|Intrudes Torres Strait Volcanic group, intruded by Badu Granite. of Badu Suite.||||||
36370|Horn Island Granite|69593|5|Briefly described|p477 Tb.6.2|||Torres Strait region: Jardine Subprovince, Kennedy Igneous Association. Associated with Au-base metal mineralisation.||Badu Suite.||||
36370|Horn Island Granite|72983|6|Mentioned|p5|Artinskian|Gzhelian|Jardine Subprovince, Kennedy Igneous Association. Considered broadly co-magmatic with the Torres Strait Volcanic Group. [ambiguous formal or informal use]|285-300 Ma K-Ar|Of Bardu Supersuite.||||
36494|Horse Camp Mill complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 107.||||||
77821|Horse Granite Gneiss|65388|4|Described|p238-240, 280, 236, 301, 340, 432|Early Carboniferous|Early Carboniferous|New name. Rawbelle Batholith, Auburn Province. Within Yerilla Metamorphics. Intrudes Yerilla Metamorphics. Intruded by Aisbetts Granodiorite. Complex interfingering relationship? Unconformably overlain by Narayen beds. Age tentative. Foliated biotite leucogneiss and mesocratic biotite ortho-gneiss.||||||
77821|Horse Granite Gneiss|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Auburn Subprovince. This unit, as well as the Mount Clairvoyant Granite, Carinya Granite and Donore Granite Gneiss, are all mapped under the same symbol, Cga.||||||
77821|Horse Granite Gneiss|68679|5|Briefly described|p312, p406, p418|Carboniferous|Carboniferous|Northern New England Orogen. Foliation/lineation detailed.||||Interfingers with Yerilla Metamorphics. Is intruded by Aisbetts Granodiorite.|Foliated biotite leucogneiss, mesocratic biotite orthogneiss.|
38243|Horse Pocket Suite|23422|5|Briefly described|p217 Table 6.11|||||||||
38243|Horse Pocket Suite|24613|5|Briefly described|p114|||Comprises only the Horse Pocket Volcanics.  Included as a separate suite as the rocks are enriched in Ba and La and depleted in Y with respect to mafic-intermediate suite. Also written as the informal Horse Pocket suite (p114).||||||07-FEB-11
38243|Horse Pocket Suite|69593|6|Mentioned|p495|Carboniferous|Carboniferous|Identified in basaltic-andesitic rocks within Carboniferous sedimentary/volcanic units in the Charters Towers region; Broken River Province.||||||
23653|Horse Pocket Volcanics|23422|5|Briefly described|p180, p205 Table 6.3|Carboniferous|Early Carboniferous|Of Glenrock Group. Also see p217, of Horse Pocket Suite.||||||
23653|Horse Pocket Volcanics|23430|5|Briefly described|p506 + p520|||Youngest member of Glenrock Group. Of Glenrock Group. Overlying Unit Ellenvale beds - unconformable.  Burdekin Basin Province.||||||
23653|Horse Pocket Volcanics|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group.||||||
23653|Horse Pocket Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V48.||||||
23653|Horse Pocket Volcanics|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
23653|Horse Pocket Volcanics|24613|2|Defined|p9 Fig. 4, p92, p99-100|Visean|Visean|Now included in Glenrock Group. Previously referred to as Wild Horse Volcanics. Conformable on Mount Douglas Fm; intruded by Emysland Granodiorite. Geological province: Burdekin Basin, occupying core of Fig Tree Syncline.Thickness: ~280m.  Andesite.||||||07-FEB-11
23653|Horse Pocket Volcanics|37573|4|Described|p225|||||||||
23653|Horse Pocket Volcanics|38658|6|Mentioned|p152|||||||||
23653|Horse Pocket Volcanics|39445|5|Briefly described|p90|||See also Table 7||||||
23653|Horse Pocket Volcanics|39686|6|Mentioned|p73|||||||||
23653|Horse Pocket Volcanics|42547|5|Briefly described|p76|||||||||
23653|Horse Pocket Volcanics|43095|6|Mentioned|p28|||of Glenrock Group?||||||
23653|Horse Pocket Volcanics|43259|4|Described|Appendix 1,p5.||Early Carboniferous|||||||
23653|Horse Pocket Volcanics|43933|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||
23653|Horse Pocket Volcanics|43935|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||22-FEB-05
23653|Horse Pocket Volcanics|68731|5|Briefly described|p187, p204|Mississippian|Mississippian|< 280 m thick. Restricted to the core of the Fig Tree Syncline on ROLLINGSTONE.||||Conformably underlain by the Mount Douglas Formation. Unconformably overlain by the Ellenvale beds.|Comprises massive, poorly sorted, andesitic breccia in which clasts range to boulder size. Massive andesite, presumably as flows, is a subordinate lithology.|14-JUL-14
36602|Horse Swamp Creek granite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Informal name. Intrudes Rudd Granite. Geological Province: Georgetown Region.||||||08-JUL-15
36602|Horse Swamp Creek granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 378.  I-Type.||||||
74233|Horseshoe Bay Granite|68901|5|Briefly described|p4, p19-21, p144|Aptian|Aptian|Northern New England Orogen, Bowen Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail. Previously included in Gloucester Granite by Allen et al. (1998).|119.5 +/- 0.7 Ma (SHRIMP U-Pb)||||Pale grey to buff, leucocratic, fine-grained, moderately porphyritic biotite syenogranite with small miarolitic cavities and traces of fluorite and altered allanite.|15-NOV-18
74233|Horseshoe Bay Granite|69594|5|Briefly described|p567, p569-570, p571 Fig.7.47|Cretaceous|Cretaceous|Bowen-Mackay region. Forms prominent outcrops. Geochemistry plots and discussion.|119.5 +/- 0.7 Ma (SHRIMP: Cross et al., 2012).||||Dominantly biotite leucogranite. Miarolitic cavities, pegmatitic patches and microgranophyric textures. Mafic enclaves scarce or absent. Contains traces of fluorite. Commonly partly altered ("iron" stained).|
74233|Horseshoe Bay Granite|71592|5|Briefly described|Appendix A.||||120+/-0.7 Ma (SHRIMP U-Pb zircon).||||Syenogranite.|
78897|Houdini Granite|67323|5|Briefly described|p18|||Subsurface. Occurs in the core of an antiformal structure. Relatively weak magnetic response.||||Surrounded by Double Crossing Metamorphics.||
78897|Houdini Granite|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Subsurface: interpreted from airborne magnetic data. Shown on Schematic Diagram as coeval with Saint Mungo and Gin Creek Granites (Wonga-Burstall Event ~1740 Ma).|||||Granite.|
78897|Houdini Granite|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Interpreted from airborne magnetic data.|||||Granite.|
78897|Houdini Granite|69591|5|Briefly described|p36, p60|||Under cover; interpreted to form the core of an antiformal structure of Double Crossing Metamorphics.||Burstall Suite.||Is surrounded by (?intrudes) Double Crossing Metamorphics.|Granite; interpreted from airborne magnetic data.|
36192|Howick Island Granite|23423|5|Briefly described|p289|||Yates Supersuite||||||
36192|Howick Island Granite|23512|5|Briefly described|Map Legend||Late Permian|of Yates Supersuite.||||||
36192|Howick Island Granite|60425|5|Briefly described|p190|Late Permian|Late Permian|Of Howick Island Suite (Yates Supersuite). Grey, medium-grained biotite granodiorite. I-type. Quartz-cassiterite-wolframite veins are present.||||||07-FEB-11
69332|Howick Island Suite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Yates Supersuite. Contains Howick Island Granodiorite. I-type.||||||07-FEB-11
26623|Hoy Basalt|30916|6|Mentioned|p100|||||||||
26623|Hoy Basalt|32493|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26623|Hoy Basalt|33144|6|Mentioned|Fig. 1|||||||||
26623|Hoy Basalt|34390|4|Described|Table 3|||Tertiary||||||
26623|Hoy Basalt|34392|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26623|Hoy Basalt|34408|6|Mentioned|p185|||On Table||||||
26623|Hoy Basalt|34717|6|Mentioned|p99|||||||||
26623|Hoy Basalt|34932|6|Mentioned|p305|||||||||
26623|Hoy Basalt|35015|6|Mentioned|p313|||||||||
26623|Hoy Basalt|37607|6|Mentioned|p338|||See also Fig.8 and P340.||||||
26623|Hoy Basalt|39212|5|Briefly described|p32|||||||||
26623|Hoy Basalt|39440|6|Mentioned|p164|||||||||
26623|Hoy Basalt|39445|5|Briefly described|Table 14|||Sapphires. See also P152||||||
26623|Hoy Basalt|41246|6|Mentioned|Map legend|Tertiary||||||||
26623|Hoy Basalt|42614|5|Briefly described|P 14|||||||||
26623|Hoy Basalt|42747|6|Mentioned|Fig.9, P38|||||||||
26623|Hoy Basalt|43029|6|Mentioned|fig.2,p16|||||||||
26623|Hoy Basalt|43085|6|Mentioned|p26|||||||||
26623|Hoy Basalt|43204|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||23-DEC-11
26623|Hoy Basalt|43213|2|Defined|p10, p19, p96, p161-163, p174-175|Miocene|Late Jurassic|See also p191-192, p239. Veevers et al. (1964). More than 70 widespread basalt plugs, up to 300m high, are associated with eroded volcaniclastic rocks thought to be the source of the abundant sapphires and zircons and rare diamonds in this region. The validity of the name is in question given the 40my time-span of the rocks: dating by Stephenson et al. (1989) and Robertson and Sutherland (1992). Fission-track dating has given a zircon age of 65.9 +/- 5.5 Ma. Geophysics described.|57-14 Ma (K-Ar whole rock).|||Intrudes Anakie Metamorphic Group and Retreat Supersuite.|Mostly massive, olivine-phyric, fine-grained basalt; also olivine dolerite, pyroclastics and local breccia. Pleonaste megacrysts are ubiquitous.|
26623|Hoy Basalt|43994|14|Not recorded|Map Legend|||||||||
26623|Hoy Basalt|43998|14|Not recorded|p15,22||Tertiary|||||||
26623|Hoy Basalt|44337|5|Briefly described|Map Legend||Tertiary|Lithology.||||||
26623|Hoy Basalt|45071|3|Fully described|Table 16|||||||||
26623|Hoy Basalt|45073|6|Mentioned|p42|||Intrudes Ducabrook Fm.||||||
26623|Hoy Basalt|48845|2|Defined|p23,38,41,44,46-50,||Tertiary|p53,Fig.10, map. Olivine basalt plug.||||||
26623|Hoy Basalt|60369|5|Briefly described|Map Legend|Tertiary|Tertiary|Olivine basalt plugs and dykes. Intrudes the Retreat Granite.||||||02-SEP-04
26623|Hoy Basalt|68482|5|Briefly described|Map Legend|Neogene|Paleogene|Shown as Tertiary in age.|||||Olivine basalt and minor gabbro and dolerite; plugs.|
26623|Hoy Basalt|69599|5|Briefly described|p644|||Veevers et al. (1964). Hoy Province. Intrudes the Retreat Batholith, the Anakie Metamorphic Group and the Drummond Basin. Regarded as a long-lived volcanic province, but its 40-million-year time span casts doubt on its validity as a unit. Over 70 plugs forming prominent conical hills up to 240m high (Mount Leura). Associated with alluvial gem (sapphire and zircon) deposits. Several age determinations given.|c.56 Ma to c.14 Ma.|||Overlies Withersfield Quartz Syenite.|Massive, fine-grained, mainly olivine-phyric basalt, with minor olivine dolerite and olivine gabbro; basanite, alkali basalt, hawaiite and minor nephelinite also occur. Most are moderately to strongly nepheline normative.|
26623|Hoy Basalt|72297|5|Briefly described|p759|||Comprises >70 eroded volcanic vent plugs that intrude the Retreat Batholith. Probable source of sapphires in the Anakie field.|||||Porphyritic olivine basalt with inclusions of basic plutonic rocks, especially peridotite.|
75117|Hudson granite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name. Of the Bedarra Suite (Bedarra Batholith or Supersuite?) in the Bedarra Granite Belt. Cream to buff, coarse-grained, highly porphyritic biotite granite; with rare inclusions (to ~10cm). I-type.||||||07-FEB-11
75629|Humbug Creek Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||White to pale grey, fine to medium-grained, uneven-grained to slightly porphyritic (muscovite-) biotite and biotite-muscovite monzogranite; moderately to strongly foliated and extensively recrystallise.|
25952|Humpy Creek Member|39493|2|Defined|p96|late Eocene|middle Eocene|Mid to late Eocene||||||
25952|Humpy Creek Member|40116|6|Mentioned|p37|||||||||
25952|Humpy Creek Member|41927|5|Briefly described|p64|||||||||
25952|Humpy Creek Member|42021|6|Mentioned|Fig.1 p320|||||||||
25952|Humpy Creek Member|71092|6|Mentioned|p232|Eocene|Eocene|||Rundle Formation.||||
25952|Humpy Creek Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
23658|Huonfels Rhyolite Member|23291|5|Briefly described|p91 Fig. 3.9|Late Carboniferous|Late Carboniferous|Parent: Dismal Creek Dacite of the Cumberland Range Volcanic Group. Thickness: 30-50m. Geological Province: Georgetown Region.||||||30-JUN-15
23658|Huonfels Rhyolite Member|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23658|Huonfels Rhyolite Member|40542|6|Mentioned|p97|||||||||
23658|Huonfels Rhyolite Member|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
23658|Huonfels Rhyolite Member|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of the Dismal Creek Dacite (Cumberland Range Volcanic Group).||||||05-JUL-04
23658|Huonfels Rhyolite Member|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron.||Shown as basal unit in Dismal Creek Dacite.|||Cream, sparsely porphyritic rhyolite; altered rhyolitic breccia, minor interbedded sandstone and siltstone.|19-MAY-15
32137|Hutchinsons Granite|23037|4|Described|p71,2|Permian|Carboniferous|Intrudes the Boam Creek Granodiorite.||||||
32137|Hutchinsons Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[COghu].  Pink to red, medium- to fine-grained biotite, granite, aplite.||||||
32137|Hutchinsons Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to red, fine- to medium-grained, biotite granite, common aplite veins; microgranite with miarolitic cavities.||||||18-MAY-04
32137|Hutchinsons Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32137|Hutchinsons Granite|65388|4|Described|p259-260, p236 Fig. 81, p237, 238, 244|Early Permian|Late Carboniferous|Intrudes Boam Creek Quartz Monzodiorite. Flanked by Torsdale Volcanics. Pink to red, medium grained biotite-hornblende granite. Age uncertain.||||||
32137|Hutchinsons Granite|68679|5|Briefly described|p404, p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Boam Creek Quartz Monzodiorite and Torsdale Volcanics.|Pink to red, medium-grained biotite-hornblende granite and microgranite with miarolitic cavities.|
24314|Idalia Rhyolite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Rhyolitic ignimbrite.  Overlies Carron Rhyolite.||||||
24314|Idalia Rhyolite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group.||||||02-JUL-04
24314|Idalia Rhyolite|23291|4|Described|p26, p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Croydon Volcanic Group. Age: 1552+/-2Ma (U-Pb), 1548+/- SHRIMP). Thickness: up to 150m? Geological Province: Georgetown Region.||||||08-JUL-15
24314|Idalia Rhyolite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V807. S-Type.||||||
24314|Idalia Rhyolite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24314|Idalia Rhyolite|40659|2|Defined|p250|Mesoproterozoic|Mesoproterozoic|||||||
24314|Idalia Rhyolite|40954|6|Mentioned|p132|||||||||
24314|Idalia Rhyolite|41975|5|Briefly described|Fig.3 P433|||||||||
24314|Idalia Rhyolite|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24314|Idalia Rhyolite|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
24314|Idalia Rhyolite|43793|5|Briefly described|p333|||U-Pb age: 1552+/-2 Ma||||||
24314|Idalia Rhyolite|50537|5|Briefly described|p3.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Geological Province: Georgetown Inlier. Age: 1552 +/- 2Ma (U-Pb).||||||
24314|Idalia Rhyolite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group.  Crystal-rich rhyolitic ignimbrite.||||||
24314|Idalia Rhyolite|63866|5|Briefly described|p78|Calymmian|Calymmian|The same sample used for the provided TIMS date was also analysed with SHRIMP techniques, yielding a crystallisation age of 1548 +/- 18 Ma (Black and Withnall, 1993).|1552 +/- 2 Ma (TIMS, Black and McCulloch, 1990)|Croydon Volcanic Group||||
24314|Idalia Rhyolite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.||Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|Conformably overlies Carron Rhyolite.|Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|Conformably overlies Carron Rhyolite.|Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|Conformably overlies Carron Rhyolite.|Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|Conformably overlies Carron Rhyolite.|Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|Conformably overlies Carron Rhyolite.|Green-grey, bluish-grey or dark grey moderately crystal-rich rhyolitic to rhyodacitic ignimbrite, 1-3 mm crystals and 1-5 mm graphite pellets; eutaxitic texture in places.|
24314|Idalia Rhyolite|68416|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Shown as younger than D2 ~ 1552 Ma.|< 1552 Ma|Of the Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|||
24314|Idalia Rhyolite|68417|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Croydon Province.||Of the Croydon Volcanic Group.|Includes Democrat Rhyolite Member.|||
24314|Idalia Rhyolite|69591|5|Briefly described|p74 Tb.2.5, p75|||Croydon Province, Georgetown Inlier. Intense recrystallisation and moderate deuteric alteration are characteristic. Up to 150m ? thick. With the Parrot Camp Rhyolite, forms about 80% of the Group's exposed area.|1548 +/- 18 Ma (Black and Withnall, 1993).|Croydon Volcanic Group.|||Crystal-rich rhyolitic ignimbrite, minor dacitic lava, ignimbrite and agglomerate. Intensely welded, extensively recrystallised, crystal-rich and pumice-poor; eutaxitic textures are absent or very obscure.|
24314|Idalia Rhyolite|71592|5|Briefly described|Appendix A.||||1548+/-18 Ma (SHRIMP U-Pb zircon).||||Ignimbrite.|
29208|Illewanna Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
29208|Illewanna Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 802. S-Type.||||||
29208|Illewanna Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
29208|Illewanna Granite|40659|6|Mentioned|p250|||||||||
29208|Illewanna Granite|40954|6|Mentioned|p133|||||||||
29208|Illewanna Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
29208|Illewanna Granite|50537|6|Mentioned|p1.3|||||||||
29208|Illewanna Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Medium-grained, slightly porphyritic garnet-biotite granite; porphyritic||||||
29208|Illewanna Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium-grained slightly porphyritic garnet-biotite granite.|28-MAY-15
29208|Illewanna Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Medium-grained slightly porphyritic garnet-biotite granite.|28-MAY-15
29208|Illewanna Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Coarse biotite granite with trace secondary muscovite; contains garnet.|
28002|Imooya Granite|23420|5|Briefly described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group and Morehead Granite||||||
28002|Imooya Granite|43596|4|Described|p35, p26 Tb. 2, p27 Tb. 3|||Of Ebagoola Suite (Kintore Supersuite).  Intrudes Sugarbag Creek Quartzite and Morehead Granite(?). V.pale grey to white muscovite-biotite to biotite-muscovite granite and leucogranite; pegmatite; aplite.||||||27-JAN-09
28002|Imooya Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
28002|Imooya Granite|72983|6|Mentioned|p41, p43|Early Devonian|late Silurian|Hosts northwest trending, Au-bearing quartz vein sets that comprise the Alice River Goldfield.||||Intruded by Alice Queen dyke.||
41260|Impey Granodiorite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Hornblende-biotite granodiorite.||||||
41260|Impey Granodiorite|65388|2|Defined|p320-321, 251, 301, 305, 306, 340|Late Permian|Middle Permian|Of Tandora Suite. Previously mapped partly as Kilbeggan Granite (Whitaker & others, 1974). Shape suggests this unit intrudes Ah Fat Granodiorite Complex and Evandale Tonalite. K-Ar (biotite) dating gave mid-Permian age  266+/-5 Ma, unlike other dated granites in area.  Dominantly pink, medium to coarse-grained, equigranular biotite granodiorite to monzogranite.||||||
41260|Impey Granodiorite|68679|4|Described|p416, p418-420|||Southern part of the Rawbelle Batholith. Ovoid; ~100 km2. Geochemistry plot.|266 +/- 5 Ma (K-Ar: Whitaker et al., 1974).|Tandora Suite.||?Intrudes surrounding Ah Fat Granodiorite Complex and Evandale Tonalite.|Hornblende-biotite granodiorite.|
25076|Ingelara Formation|13516|5|Briefly described|p145 fig 3, p146 fig 4, p152 fig 6, p156|Late Permian|Late Permian|From Denison Trough, Bowen Basin. Age APP5004||||||
25076|Ingelara Formation|22601|4|Described|401,413, 414, 418|Permian|Permian|Geol province Bowen Basin. Overlying unit Catherine Sandstone, underlying unit Freitag Formation.||||||07-APR-09
25076|Ingelara Formation|22872|5|Briefly described|p535, Fig.1 p536|Early Triassic|Late Permian|||||||
25076|Ingelara Formation|22973|5|Briefly described|p11 Fig.2(e)|Late Permian|Late Permian|||||||
25076|Ingelara Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
25076|Ingelara Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
25076|Ingelara Formation|22978|6|Mentioned|p148 Fig.1|||||||||
25076|Ingelara Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
25076|Ingelara Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
25076|Ingelara Formation|23444|5|Briefly described|p190|Triassic|Permian|||||||
25076|Ingelara Formation|24069|5|Briefly described|p284|Permian|Permian|Geological Province: Bowen Basin.||||||
25076|Ingelara Formation|24077|5|Briefly described|p410 Tb. 2|Early Permian|Early Permian|Of the Gebbie Subgroup.  Mudstone with  'floating' grains and 'erratic' pebbles, thin calcareous sandstone, thin limestone and coquinite.  Max. thickness: 200m.  Geological Province: Bowen Basin.||||||
25076|Ingelara Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: >259Ma.  Geological Province: Bowen Basin.||||||
25076|Ingelara Formation|24491|5|Briefly described|p20|||Geological Province: Bowen Basin.||||||
25076|Ingelara Formation|29391|6|Mentioned|Table 3|||See P18.||||||
25076|Ingelara Formation|29393|6|Mentioned|Table 2|||Permian.||||||
25076|Ingelara Formation|29410|6|Mentioned|p274|||Geological map. Permian.||||||
25076|Ingelara Formation|29412|5|Briefly described|p209|||See also Fig.2.||||||
25076|Ingelara Formation|29721|6|Mentioned|Table 65|||||||||
25076|Ingelara Formation|30153|6|Mentioned|p151|||||||||
25076|Ingelara Formation|30340|6|Mentioned|p2532|||Lithology||||||
25076|Ingelara Formation|30341|5|Briefly described|p136|||Lower Permian age||||||
25076|Ingelara Formation|30449|6|Mentioned|p4|||Brachiopods. See also P8,12,13||||||
25076|Ingelara Formation|30450|6|Mentioned|Table 1|||Permian age. Southwest Bowen Basin||||||
25076|Ingelara Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
25076|Ingelara Formation|30545|6|Mentioned|Fig.2|||Lower Permian||||||
25076|Ingelara Formation|30546|6|Mentioned|p107|||Correlation. Lower Permian age.||||||
25076|Ingelara Formation|30826|6|Mentioned|p634|||||||||
25076|Ingelara Formation|30850|6|Mentioned|p343|||||||||
25076|Ingelara Formation|30852|4|Described|p173|||||||||
25076|Ingelara Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
25076|Ingelara Formation|30916|6|Mentioned|p98|||Table on P98||||||
25076|Ingelara Formation|31079|6|Mentioned|Fig. 6|||||||||
25076|Ingelara Formation|31115|6|Mentioned|p32|||Permian||||||
25076|Ingelara Formation|31120|4|Described|p151|||See also P152. Correlative.||||||
25076|Ingelara Formation|31303|5|Briefly described|p289|||See also Table 1||||||
25076|Ingelara Formation|31304|5|Briefly described|p624|||Mention stratigraphy||||||
25076|Ingelara Formation|31305|4|Described|p568|||Mention Table 1||||||
25076|Ingelara Formation|31531|6|Mentioned|p11|||||||||
25076|Ingelara Formation|31621|6|Mentioned|p151|||||||||
25076|Ingelara Formation|31690|6|Mentioned|p37|||Correlation. See also Fig. 2||||||
25076|Ingelara Formation|32096|6|Mentioned|p574|||||||||
25076|Ingelara Formation|32139|6|Mentioned|p582|||||||||
25076|Ingelara Formation|32577|4|Described|p23|||L.Perm. See also P24,33,34,42.||||||
25076|Ingelara Formation|32578|6|Mentioned|p350|||Refers Traves (1971)||||||
25076|Ingelara Formation|32689|6|Mentioned|Fig.2|||Name extended into German Ck. area||||||
25076|Ingelara Formation|32840|6|Mentioned|Fig.1|||Stratigraphy & biostratigraphy. See also P30||||||
25076|Ingelara Formation|32943|6|Mentioned|p88|||||||||
25076|Ingelara Formation|32945|6|Mentioned|p81|||See also PP82,90 & Fig.2||||||
25076|Ingelara Formation|33059|4|Described|Table 1|||L.Perm.||||||
25076|Ingelara Formation|33366|6|Mentioned|Fig.3|||Perm.||||||
25076|Ingelara Formation|33390|4|Described|p3|||||||||
25076|Ingelara Formation|33530|5|Briefly described|Table 1|||Lower Permian||||||
25076|Ingelara Formation|33701|6|Mentioned|Fig.1|||L.Perm.||||||
25076|Ingelara Formation|33711|6|Mentioned|p383|||||||||
25076|Ingelara Formation|33745|6|Mentioned|Fig.2|||See also Figs 3, 6 & 7||||||
25076|Ingelara Formation|33981|5|Briefly described|p574|||||||||
25076|Ingelara Formation|34132|6|Mentioned|p2|||Upper Permian||||||
25076|Ingelara Formation|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
25076|Ingelara Formation|34170|6|Mentioned|p48|||Lower Permian. Artinskian||||||
25076|Ingelara Formation|34390|4|Described|Table 2|||Permian||||||
25076|Ingelara Formation|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25076|Ingelara Formation|34568|6|Mentioned|p220|||Bowen Basin. Fauna||||||
25076|Ingelara Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
25076|Ingelara Formation|35079|6|Mentioned|Fig.3|||||||||
25076|Ingelara Formation|35145|6|Mentioned|p83|||||||||
25076|Ingelara Formation|35148|4|Described|p411|||See also Table 1.||||||
25076|Ingelara Formation|35150|6|Mentioned|p420|||||||||
25076|Ingelara Formation|35284|6|Mentioned|p17|||||||||
25076|Ingelara Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
25076|Ingelara Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
25076|Ingelara Formation|35822|6|Mentioned|p40|||||||||
25076|Ingelara Formation|35845|6|Mentioned|Fig.25|||||||||
25076|Ingelara Formation|35873|6|Mentioned|Fig.25|||||||||
25076|Ingelara Formation|36103|4|Described|Table 1|||||||||
25076|Ingelara Formation|36104|6|Mentioned|p122|||||||||
25076|Ingelara Formation|36233|5|Briefly described|p157|||See also Table 1.||||||
25076|Ingelara Formation|36241|4|Described|p123|||||||||
25076|Ingelara Formation|36243|6|Mentioned|Table 3A|||||||||
25076|Ingelara Formation|36739|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|37070|4|Described|p72|||||||||
25076|Ingelara Formation|37072|5|Briefly described|p90|||||||||
25076|Ingelara Formation|37446|5|Briefly described|p187|||||||||
25076|Ingelara Formation|37450|6|Mentioned|p374|||||||||
25076|Ingelara Formation|37610|6|Mentioned|p302|||See also Fig.4.||||||
25076|Ingelara Formation|37705|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|37724|6|Mentioned|Table 1|||||||||
25076|Ingelara Formation|37726|3|Fully described|p147|||||||||
25076|Ingelara Formation|37918|6|Mentioned|p455|||||||||
25076|Ingelara Formation|38092|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|38204|6|Mentioned|p80|||||||||
25076|Ingelara Formation|38312|4|Described|p461|||||||||
25076|Ingelara Formation|38586|6|Mentioned|p26|||||||||
25076|Ingelara Formation|38917|6|Mentioned|p162|||||||||
25076|Ingelara Formation|38955|4|Described|p314|||||||||
25076|Ingelara Formation|39212|4|Described|p34|||Excursion site described. See also P11 & 35||||||
25076|Ingelara Formation|39219|6|Mentioned|p46|||Microflora||||||
25076|Ingelara Formation|39252|6|Mentioned|Fig.13|||||||||
25076|Ingelara Formation|39261|6|Mentioned|Fig.6|||||||||
25076|Ingelara Formation|39262|6|Mentioned|p126|||||||||
25076|Ingelara Formation|39263|6|Mentioned|Fig.1|||||||||
25076|Ingelara Formation|39264|6|Mentioned|Fig. 4|||||||||
25076|Ingelara Formation|39267|6|Mentioned|p238|||||||||
25076|Ingelara Formation|39268|6|Mentioned|p270|||||||||
25076|Ingelara Formation|39272|5|Briefly described|p295|||Correlation||||||
25076|Ingelara Formation|39273|6|Mentioned|p305|||||||||
25076|Ingelara Formation|39275|6|Mentioned|p332|||||||||
25076|Ingelara Formation|39412|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|39423|6|Mentioned|p47|||||||||
25076|Ingelara Formation|39445|5|Briefly described|Table 8|||||||||
25076|Ingelara Formation|39494|6|Mentioned|Fig.5|||||||||
25076|Ingelara Formation|39611|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|39813|6|Mentioned|Map legend|Permian|Permian|Permo Carboniferous||||||
25076|Ingelara Formation|39815|6|Mentioned|Fig.10|||||||||
25076|Ingelara Formation|39943|6|Mentioned|Table 5A|||||||||
25076|Ingelara Formation|39994|6|Mentioned|p200|||||||||
25076|Ingelara Formation|40030|6|Mentioned|Fig.5|||||||||
25076|Ingelara Formation|40093|6|Mentioned|p40|||||||||
25076|Ingelara Formation|40250|6|Mentioned|Table 6|||||||||
25076|Ingelara Formation|40256|6|Mentioned|p306|||||||||
25076|Ingelara Formation|40539|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|40544|6|Mentioned|Fig.6|||||||||
25076|Ingelara Formation|41173|6|Mentioned|Table 2|||||||||
25076|Ingelara Formation|41246|6|Mentioned|Map legend|Permian||||||||
25076|Ingelara Formation|41247|6|Mentioned|Fig.7|||||||||
25076|Ingelara Formation|41275|4|Described|p30|||||||||
25076|Ingelara Formation|41330|6|Mentioned|Table 1|||||||||
25076|Ingelara Formation|41514|6|Mentioned|p83|||||||||
25076|Ingelara Formation|41605|6|Mentioned|Fig.2|||||||||
25076|Ingelara Formation|41666|6|Mentioned|p1|||||||||
25076|Ingelara Formation|41737|6|Mentioned|p351|||||||||
25076|Ingelara Formation|42249|6|Mentioned|Table 1 P22|||||||||
25076|Ingelara Formation|42250|6|Mentioned|p33|||||||||
25076|Ingelara Formation|42251|6|Mentioned|Fig.2 P38|||||||||
25076|Ingelara Formation|42253|5|Briefly described|Fig.2 P217|||||||||
25076|Ingelara Formation|42254|6|Mentioned|p221|||||||||
25076|Ingelara Formation|42437|6|Mentioned|Fig.3 P822|||||||||
25076|Ingelara Formation|42578|5|Briefly described|Table 1 P124-125|||||||||
25076|Ingelara Formation|42611|6|Mentioned|P 11|||||||||
25076|Ingelara Formation|42614|5|Briefly described|p13|||Bowen Basin. See also misspelt Ingalara Formation.||||||
25076|Ingelara Formation|42621|6|Mentioned|p274|||||||||
25076|Ingelara Formation|42641|6|Mentioned|Fig.3 P110|||||||||
25076|Ingelara Formation|42662|6|Mentioned|p84 Fig.4|||||||||
25076|Ingelara Formation|42865|5|Briefly described|p18|||||||||
25076|Ingelara Formation|42911|6|Mentioned|p9|||||||||
25076|Ingelara Formation|42994|6|Mentioned|p235|||||||||
25076|Ingelara Formation|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
25076|Ingelara Formation|43017|5|Briefly described|Fig.3,p375|||||||||
25076|Ingelara Formation|43050|5|Briefly described|p4|||see also Fig.1,p5.||||||
25076|Ingelara Formation|43185|6|Mentioned|6-10||Late Permian|||||||
25076|Ingelara Formation|43474|14|Not recorded|p69,100|||||||||
25076|Ingelara Formation|43475|14|Not recorded|p553||Permian|||||||
25076|Ingelara Formation|43580|6|Mentioned|p360||Permian|||||||
25076|Ingelara Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
25076|Ingelara Formation|43737|6|Mentioned|p5||Kungurian|||||||
25076|Ingelara Formation|43812|6|Mentioned|Fig.3,p145|||||||||
25076|Ingelara Formation|43977|14|Not recorded|p576-578|||||||||
25076|Ingelara Formation|43982|14|Not recorded|Map Legend|||||||||
25076|Ingelara Formation|43987|14|Not recorded|p267,270|||||||||
25076|Ingelara Formation|43990|14|Not recorded|Map Legend|||Part of Gebbie Sub-Group.||||||
25076|Ingelara Formation|43994|14|Not recorded|Map Legend|||||||||
25076|Ingelara Formation|44022|14|Not recorded|Map Legend||Early Permian|||||||
25076|Ingelara Formation|44023|4|Described|Tb.2,p6||Early Permian|||||||
25076|Ingelara Formation|44079|14|Not recorded|p50|||||||||
25076|Ingelara Formation|44085|2|Defined|Opp.p4,10,map|||||||||
25076|Ingelara Formation|44091|14|Not recorded|not on card|||Part Middle Bowen Group in Springsure area.||||||
25076|Ingelara Formation|44115|14|Not recorded|p19,21|||||||||
25076|Ingelara Formation|44169|2|Defined|Tb.1,p6,7,map|||||||||
25076|Ingelara Formation|44170|4|Described|p6,10-11,9,30,33,|||Tb.1||||||
25076|Ingelara Formation|44172|2|Defined|p1327-8,1330,1332-3,||Artinskian|p1337,1343,Fig.2,Tb.1. Springsure area.||||||
25076|Ingelara Formation|44173|14|Not recorded|p109-113||Early Permian|Conformably overlies Freitag Formation.||||||
25076|Ingelara Formation|44208|14|Not recorded|p94||Permian|See also Lexicon.||||||
25076|Ingelara Formation|44218|14|Not recorded|p19||Kungurian|Middle Kungurian.||||||
25076|Ingelara Formation|44219|14|Not recorded|p31||Artinskian|||||||
25076|Ingelara Formation|44311|14|Not recorded|p199,201|||Contains Strophalosia typica (Booker)||||||
25076|Ingelara Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
25076|Ingelara Formation|44350|14|Not recorded|p52|||||||||
25076|Ingelara Formation|44419|14|Not recorded|p272,273|||||||||
25076|Ingelara Formation|44421|14|Not recorded|p4,8,9,||Permian|||||||
25076|Ingelara Formation|44422|14|Not recorded|p150,152||Early Permian|||||||
25076|Ingelara Formation|44424|14|Not recorded|p293-301|||Appears to correspond to middle unit of Gebbie Subgroup.||||||
25076|Ingelara Formation|44427|14|Not recorded|p166|||Sprinsure area.||||||
25076|Ingelara Formation|44488|14|Not recorded|p48|||||||||
25076|Ingelara Formation|44604|14|Not recorded|Fig.2,opp.p116|||||||||
25076|Ingelara Formation|44618|14|Not recorded|p514,517||Permian|||||||
25076|Ingelara Formation|44651|14|Not recorded|p117|||||||||
25076|Ingelara Formation|44857|14|Not recorded|p97||Permian|||||||
25076|Ingelara Formation|45016|14|Not recorded|p.170|||Correlated with Wandagee Formation.||||||
25076|Ingelara Formation|45031|14|Not recorded|p9,Fig.3||Permian|||||||
25076|Ingelara Formation|45071|3|Fully described|Table 6|||||||||
25076|Ingelara Formation|46849|6|Mentioned|p192|||||||||
25076|Ingelara Formation|46989|5|Briefly described|Table 1|||||||||
25076|Ingelara Formation|48600|14|Not recorded|p32|||||||||
25076|Ingelara Formation|48626|4|Described|p1,3,22,24-5,33-5,50||Permian|p52,55,93,94,Pl.1,Fig.1,2.||||||
25076|Ingelara Formation|48630|14|Not recorded|p1,4-6,18,19,Pls.1,2|||||||||
25076|Ingelara Formation|48831|14|Not recorded|p.15,23|||||||||
25076|Ingelara Formation|48841|14|Not recorded|p20|||||||||
25076|Ingelara Formation|48845|14|Not recorded|p37,38|||||||||
25076|Ingelara Formation|48847|14|Not recorded|Pl.2|||||||||
25076|Ingelara Formation|48898|6|Mentioned|Fig.4|||L.Permian. Gebbie Subgroup||||||
25076|Ingelara Formation|48900|2|Defined|p35|Early Permian|Early Permian|||||||
25076|Ingelara Formation|48919|5|Briefly described|p17|||Lower Permian||||||
25076|Ingelara Formation|48920|6|Mentioned|p84|||On Fig.B||||||
25076|Ingelara Formation|48995|6|Mentioned|Fig.3|||||||||
25076|Ingelara Formation|49644|5|Briefly described|Table|||||||||
25076|Ingelara Formation|60286|4|Described|p274|Late Permian|Late Permian|Overlies Freitag Formation. Marine mudrock. Overlain conformably by Catherine Sandstone and German Creek Formation. Geological Province: Bowen Basin.||||||09-FEB-05
25076|Ingelara Formation|60330|5|Briefly described|p261 Fig.2|Kazanian|Kazanian|||||||
25076|Ingelara Formation|61609|6|Mentioned|p240|Permian|Permian|Underlain by Aldebaran Sandstone and Freitag Formation. Geological Province: Denison Trough.||||||07-FEB-11
25076|Ingelara Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
25076|Ingelara Formation|61778|5|Briefly described|p239||Late Permian|Geological Province: Bowen Basin.||||||07-FEB-11
25076|Ingelara Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Bowen Basin.||||||
25076|Ingelara Formation|63713|5|Briefly described|p1507 Fig.2, p1508, p1522-1523, p1526|Wordian|Roadian|See also p1528-1531, p1533. Denison Trough, Bowen Basin. Graphic log. Well-log correlation.||||Overlies Aldebaran Sandstone and Freitag Formation. Is overlain by Catherine Sandstone.|Mudrock-dominated.|
25076|Ingelara Formation|63773|6|Mentioned|p1059|||||||||
25076|Ingelara Formation|63832|6|Mentioned|p131 fig 2, p137|Wordian|Wordian|West Bowen Basin. Appears in Fig.2 as Cath./Freit./Ing. Contains distal glaciomarine facies (outsized basement clasts in mudrock, glendonites) recording the final (P4) Paleozoic glaciation.||||||13-DEC-17
25076|Ingelara Formation|64631|6|Mentioned|p48 Fig.4, p49.|Wordian|Wordian|Bowen Basin. Contains distal glaciomarine facies, eg glendonites and outsized basement clasts in mudrocks. See also p44 where shown with Catherine Sst, Freitag Fm. Some biostratigraphic age control indicated.||||||
25076|Ingelara Formation|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Bowen Basin.||||Overlies Aldebaran Sandstone.||
25076|Ingelara Formation|64857|6|Mentioned|p119, p113 Fig.3|Late Permian|Late Permian|Denison Trough, Bowen Basin.||||||
25076|Ingelara Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Denison Trough, Bowen Basin. Underlies Catherine Formation and overlies Freitag Formation.||||||14-SEP-09
25076|Ingelara Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Denison Trough. Underlies Catherine Formation, overlies Freitag Formation.||||||
25076|Ingelara Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
25076|Ingelara Formation|65115|5|Briefly described|p414, 415, Fig 2 p403|Kazanian|Ufimian|Overlies the Freitag Formation, underlies the Catherine Formation in the Dension Trough, Bowen Basin. Part of Supersequence D.||||||
25076|Ingelara Formation|65116|5|Briefly described|p447, Fig 2 p436|Late Permian|Late Permian|Underlies the Catherine Formation and Overlies the Freitag Formation in the Denison Trough, Bowen Basin. Equivalent age to Trinkey Formation (Gunnedah Basin?), based on palynology.||||||
25076|Ingelara Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|?Underlies the Catherine Sandstone,  ?overlies the Freitag Formation, Denison Trough, Bowen Basin.||||||06-MAR-12
25076|Ingelara Formation|65388|6|Mentioned|p170, 172|||South west Bowen Basin. Correlated with Barfield Formation, lower Flat Top Formation .||||||
25076|Ingelara Formation|66615|6|Mentioned|p2 Fig.1|||Denison Trough, Bowen Basin.||||||
25076|Ingelara Formation|67402|6|Mentioned|p21, p23 fig CTM3|Capitanian|Capitanian|Bowen Basin. Deposited in a shallow marine environment. Forms extensive regional seals for the underlying Aldebaran Sandstone and Freitag Formation reservoirs. See also p64, p65, p66 fig BWW4, p68, p69, p72, p73, p76, p302.||||Overlies the Aldebaran Sandstone, Upper and the Freitag Formation. Overlain by the Catherine Sandstone, Black Alley Shale and the Peawaddy Formation.|Sandy siltstone, silty sandstone, shale and minor tuff.|
25076|Ingelara Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Peawaddy Formation, or Catherine Sandstone? Underlain by Freitag Formation.||
25076|Ingelara Formation|68576|5|Briefly described|Q_4: p3|Lopingian|Lopingian|Bowen Basin.||||Overlies Freitag Formation. Is overlain by Catherine Sandstone.||
25076|Ingelara Formation|68679|5|Briefly described|p350, p378, p380-382|Permian|Permian|Mollan et al. (1969). Western Bowen Basin. 200m thick. Offshore marine sediments. Mentioned as having the same fossil species as, and thus establishing the age of, the Warminster Formation (Yarrol Province).||||Overlies Freitag Formation. Passes laterally into Maria Formation. Is overlain by Catherine Sandstone and Peawaddy Formation.|Mudstone, siltstone, minor tuffs; marine fossils.|
25076|Ingelara Formation|68731|6|Mentioned|p201 Fig 3.110|Late Permian|Late Permian|Bowen Basin.||||||
25076|Ingelara Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Bowen Basin. CA-TIMS age of 257.3 Ma (Nicoll etal., 2015). Corresponding to APP5 zone (Lopingian).||||||
25076|Ingelara Formation|71265|5|Briefly described|p589-590, p595, p606|Changhsingian|Wuchiapingian|Bowen and eastern Galilee Basins. Tidal deposits.||||Overlies Freitag Formation. Is overlain by Catherine Sandstone.|Tidal sediments with abrupt, subangular, matrix-supported conglomerates.|
25076|Ingelara Formation|71276|5|Briefly described|p287-288, p294, p295 Fig.8, p296-297|Lopingian|Lopingian|Eastern side of the Springsure Shelf (Denison Trough, Bowen Basin). Probable lateral equivalent of (part of) the Colinlea Sandstone. Marine deposits. In the Bowen Basin, this unit is known as the Maria and Blenheim Formations.||||Overlies Freitag Formation. Is overlain by Catherine Sandstone.||
25076|Ingelara Formation|71701|5|Briefly described|p155-p156, p168|Changhsingian|Wuchiapingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Freitag Formation. Overlain by the Catherine Sadnstone. Equivalent to the Rodney Creek Sandstone.||
25076|Ingelara Formation|72088|5|Briefly described|p8, p20, p38, p91|Wuchiapingian|Wuchiapingian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Freitag Formation. Overlain by the Catherine Sandstone.||
25076|Ingelara Formation|73303|6|Mentioned|p68|Wuchiapingian|Wuchiapingian|Bowen Basin. Ingelarella ingelarensis brachiopod not found stratigraphically higher than the lower Ingelara Formation (Campbell, 1960). Tuff dated to 257.3 +/- 0.5 Ma in upper Ingelara Formation (Nicoll et al., 2015).|257.3 +/- 0.5 Ma|||||
25076|Ingelara Formation|73304|6|Mentioned|p77-78|||Bowen Basin.||||||
25076|Ingelara Formation|73472|6|Mentioned|p115|Wuchiapingian|Wuchiapingian|Galilee Basin.||||Underlain by Freitag Formation. Overlain by Catherine Sandstone. Equivalent to Colinlea Sandstone.||
25076|Ingelara Formation|73625|6|Mentioned|p2-3, 13|Permian|Permian|Bowen Basin.||||Overlies Freitag Formation. Is overlain by Catherine Sandstone and (locally) Peawaddy Formation.||
36184|Ingham Granite Complex|23497|5|Briefly described|Table 1|Early Permian|Late Carboniferous|Part of the I-type Ingham Supersuite. of Kennedy Province.||||||21-JUN-13
36184|Ingham Granite Complex|23503|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
36184|Ingham Granite Complex|23507|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
36184|Ingham Granite Complex|23617|3|Fully described|p16 Table 2|Early Permian|Late Carboniferous|299 to 296 Ma (K-Ar). Also see p28-29 + p52 Table 3. Kennedy Province.||||||
36184|Ingham Granite Complex|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36184|Ingham Granite Complex|60425|5|Briefly described|p58 Tb. 4|||Part of the Ingham Batholith in the Ravenshoe-Ingham Belt, and I-type Ingham Supersuite.||||||07-FEB-11
36184|Ingham Granite Complex|68481|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Kennedy Province.||||Intrudes Kangaroo Hills Formation.|Pale grey to pale pink, fine to medium-grained porphyritic hornblende-biotite and biotite monzogranite and granodiorite; undivided granites of the northern Ingham Batholith (I-types).|
36184|Ingham Granite Complex|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
36184|Ingham Granite Complex|73450|6|Mentioned|p103, p105|Permian|Carboniferous|||||||
36357|Ingham Supersuite|23497|6|Mentioned|Table 1|||||||||
36357|Ingham Supersuite|23617|5|Briefly described|p55|||||||||
36357|Ingham Supersuite|60425|5|Briefly described|p58 Tb. 4, p100|||Part of the Ingham Batholith in the Ravenshoe-Ingham Belt together with Hinchinbrook Supersuite. I-type granite rocks.||||||07-FEB-11
36357|Ingham Supersuite|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit (in part), as well as the Claret Creek, Glenmore, Almaden, O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk. It is also mapped (in part), as CPgk, with the Badu Suite and parts of the Almaden, Leichhardt, O'Briens Creek and Ootann Supersuites, and various ungrouped Carboniferous-Early Permian plutonic units. ||||||
22001|Inkerman Metamorphics|43120|3|Fully described|p365|Early Paleozoic|Proterozoic|||||||07-NOV-08
22001|Inkerman Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Connors Subprovince. This unit, as well as the Mount Cavana beds and Key Creek Gneiss, are all mapped under the symbol, DCi.||||||
22001|Inkerman Metamorphics|68679|6|Mentioned|p347, p364|Carboniferous|Late Devonian|Northern New England Orogen.||||||
22001|Inkerman Metamorphics|68901|6|Mentioned|p2 Fig. i|Carboniferous|Late Devonian|New England Orogen.
||||||26-SEP-18
22001|Inkerman Metamorphics|69952|6|Mentioned|p85|Carboniferous|Late Devonian|||||||
27438|Inorunie Group|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
27438|Inorunie Group|22533|6|Mentioned|p54,p56|Mesoproterozoic|Mesoproterozoic|||||||
27438|Inorunie Group|22669|6|Mentioned|Fig1 P248||Mesoproterozoic|||||||
27438|Inorunie Group|22811|6|Mentioned|p605|||In Croydon Province.||||||16-JAN-07
27438|Inorunie Group|23291|4|Described|p27, p83 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Intruded by Wallys Dolerite. Underlain by Croydon Volcanic Group. Geological Province: Georgetown Region.||||||16-JAN-07
27438|Inorunie Group|23430|5|Briefly described|p456|||Underlain by Croydon Volcanic Group - unconformable. In Croydon Province.||||||16-JAN-07
27438|Inorunie Group|23453|5|Briefly described|p10 Fig.1|Early Paleozoic|Mesoproterozoic|||||||07-NOV-08
27438|Inorunie Group|23510|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|||||||
27438|Inorunie Group|24197|5|Briefly described|p76|Mesoproterozoic|Mesoproterozoic|Overlies the Croydon Volcanic Group therefore age is inferred to be Mesoproterozoic Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
27438|Inorunie Group|40218|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
27438|Inorunie Group|40860|6|Mentioned|p109|||||||||
27438|Inorunie Group|41975|3|Fully described|p438|||||||||
27438|Inorunie Group|43664|6|Mentioned|Fig.3,p15|Early Paleozoic|Proterozoic|||||||07-NOV-08
27438|Inorunie Group|43729|5|Briefly described|p3|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
27438|Inorunie Group|50537|6|Mentioned|p1.1|||Geological Province: Georgetown Inlier. Overlies: Croydon Volcanic group, Esmeralda Supersuite.||||||
27438|Inorunie Group|61258|5|Briefly described|p387 Fig. 1|Paleoproterozoic|Neoproterozoic|Geological Province: Georgetown Inlier.||||||07-NOV-08
27438|Inorunie Group|63866|5|Briefly described|p79, p81|||Deposited in a fluviatile environment. Age of the group is unknown.||||Overlies the Croydon Volcanic Group.|Sandstones, siltstone and mudstones.|
27438|Inorunie Group|65887|5|Briefly described|p40 Fig.1|Early Paleozoic|Mesoproterozoic|||||||
27438|Inorunie Group|66800|6|Mentioned|p925.|||Fluvial deposits.||||||
27438|Inorunie Group|67430|6|Mentioned|p25|||||||||
27438|Inorunie Group|68307|5|Briefly described|p78, p88, p97|Mesoproterozoic|Mesoproterozoic|North Australian Craton. Very thin, subhorizontal and with relatively flat base.||||||
27438|Inorunie Group|68355|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin. Has low K, Th and U radiometric responses.|||Includes Dirie and Guela Sandstones, and Chulcee and Arrongulla Formations.|||
27438|Inorunie Group|68356|5|Briefly described|Map legend.|Early Paleozoic|Proterozoic|Inorunie Basin. Has low K, Th and U radiometric responses.|||Includes Dirie and Guela Sandstones, and Chulcee and Arrongulla Formations.|||
27438|Inorunie Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Inorunie Basin.||||||
27438|Inorunie Group|68576|6|Mentioned|Q_11: p2|||||||||
27438|Inorunie Group|69591|5|Briefly described|p62, p75, p98|||Preserved in a small (20 x 15 km), partly fault-bounded basinal structure. Probably no more than 1500m thick. Probably a terrestrial, fluvial environment.|||Arrongulla, Chulcee Formations; Guela, Dirie Sandstones.|Disconformably overlies the Croydon Volcanic Group.|Strongly indurated quartzose sandstone (with common trough cross-bedding), micaceous sublithic sandstone, siltstone and mudstone.|
27438|Inorunie Group|70207|6|Mentioned|p14||Mesoproterozoic|Georgetown region. Minimum age given as Early Paleozoic?.||||||
27438|Inorunie Group|72381|5|Briefly described|p779|||Geological province: North Australian Craton. Part of a series of basins deposited along the eastern margin of Proterozoic Australia-Antarctica during lithospheric extension related to the rifting of Proterozoic Australia and Laurentia (Mulder et al., 2015).||||||04-OCT-19
27438|Inorunie Group|73642|6|Mentioned|p3 Fig.2, p10 Fig.8|||Georgetown Inlier.|||||Sedimentary rocks.|
25957|Insolvency Gully Formation|23422|4|Described|p183, p205 Table 6.3|Late Carboniferous|Late Carboniferous|Defined by Wyatt et al. (1970). Maximum thickness: ~1000m.||||||
25957|Insolvency Gully Formation|23430|4|Described|p504 Table 14.5 +p520|||||||||
25957|Insolvency Gully Formation|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
25957|Insolvency Gully Formation|23893|5|Briefly described|p19|Early Permian|Late Carboniferous|||||||
25957|Insolvency Gully Formation|24612|5|Briefly described|p9 Fig.2|Early Permian|Late Carboniferous|Geological Province: Burdekin Basin.||||||
25957|Insolvency Gully Formation|24613|5|Briefly described|p6 Fig. 3|Early Devonian|Precambrian|Geological province: Burdekin Basin.||||||07-FEB-11
25957|Insolvency Gully Formation|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25957|Insolvency Gully Formation|32169|6|Mentioned|Table 2|||U.Carboniferous||||||
25957|Insolvency Gully Formation|32553|4|Described|p44|||||||||
25957|Insolvency Gully Formation|35811|6|Mentioned|Fig.3|||||||||
25957|Insolvency Gully Formation|36061|4|Described|Fig.2|||||||||
25957|Insolvency Gully Formation|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
25957|Insolvency Gully Formation|37573|6|Mentioned|p226|||||||||
25957|Insolvency Gully Formation|37613|6|Mentioned|p249|||See also Fig.3||||||
25957|Insolvency Gully Formation|39445|5|Briefly described|Table 7|||||||||
25957|Insolvency Gully Formation|39686|6|Mentioned|p73|||||||||
25957|Insolvency Gully Formation|39735|6|Mentioned|p18|||||||||
25957|Insolvency Gully Formation|41774|6|Mentioned|Table 1|||||||||
25957|Insolvency Gully Formation|42295|5|Briefly described|Fig.2 P5|||||||||
25957|Insolvency Gully Formation|42547|5|Briefly described|p76|||||||||
25957|Insolvency Gully Formation|42689|5|Briefly described|map legend|Carboniferous||||||||
25957|Insolvency Gully Formation|43095|3|Fully described|p76||Late Carboniferous|Resembles & is probably equivalent to parts of the Ellenvale beds to the SE and the Marshs Creek Formation 60km NW.||||||21-MAY-04
25957|Insolvency Gully Formation|43589|6|Mentioned|p24|||Mingoom Granite is faulted against this unit.||||||23-APR-08
25957|Insolvency Gully Formation|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
25957|Insolvency Gully Formation|44061|4|Described|Table 3||Late Carboniferous|||||||
25957|Insolvency Gully Formation|45151|5|Briefly described|Table 7|||||||||
25957|Insolvency Gully Formation|46845|6|Mentioned|p143|||||||||
25957|Insolvency Gully Formation|48904|2|Defined|p41|Late Carboniferous|Late Carboniferous|||||||
25957|Insolvency Gully Formation|63154|5|Briefly described|p285 Fig. 5|Carboniferous|Carboniferous|Geological province: Charters Towers Province.||||||
25957|Insolvency Gully Formation|66529|5|Briefly described|p24, p30  |Late Carboniferous|Late Carboniferous|||||Unconformably overlies the Saint James Volcanics and Watershed North Rhyolite. Intruded by the Speed Creek Granite.|Carbonaceous/pyritic shales and sandstones.|
25957|Insolvency Gully Formation|68419|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Insolvency Graben. Minimum age shown as Early Permian.|`||||Lithofeldspathic sandstone, conglomerate, dark grey mudstone, siltstone and chert (tuff?).|
25957|Insolvency Gully Formation|68420|5|Briefly described|Map Legend|Early Permian|Carboniferous|Of the Insolvency Graben. Of the Kennedy Province.|||||Lithofeldspathic sandstone, conglomerate, dark grey mudstone, siltstone and chert (tuff?).|
25957|Insolvency Gully Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Balfes Creek, Ellenvale and Wade beds; Marshs Creek Formation; and Silver Valley Conglomerate, are all mapped under the symbol, CPs.||||||
25957|Insolvency Gully Formation|68731|5|Briefly described|p204|Pennsylvanian|Pennsylvanian|Wyatt et al. (1970); Gunther and Withnall (1992). Occupies 15 km2 on ROLLINGSTONE. ~ 1000 m thick. Calamites in this unit, and its unconformable relationship with the Saint James Volcanics assigned as Mississippian, suggests a Pennsylvanian age.|||||Comprises a succession of conglomerate, lithofeldspathic sandstone, and siltstone and conglomerate.|
25957|Insolvency Gully Formation|69593|5|Briefly described|p495-496|Permian|Late Carboniferous|Townsville hinterland. Younger age may be Late Carboniferous.|||||Crystal-rich rhyolitic ignimbrite, rhyolite lava, volcaniclastic and epiclastic rocks, and other sediments; minor mafic rocks.|
40124|Inverness Volcanics|24615|5|Briefly described|CD|Permian|Permian|[Pvi].  Dark grey trachyte to dacite, volcanic breccia; numerous small hornblende quartz monzodiorite intrusions.||||||
40124|Inverness Volcanics|50197|5|Briefly described|Map legend|Permian|Permian|||||||
40124|Inverness Volcanics|68008|2|Defined|p70, p147, p182-184, p376, p627|Permian|Permian|Defined here (Murray et al., 2012). Named after the property Inverness. Type section is along upper Smoky Creek, from GR255900E 7333100N. Crops out over 5km square. Previously mapped by Dear et al. (1971) as the easternmost part of the Mount Gerard Complex. Geochemistry described: possibly comagmatic with Craiglands Quartz Monzodiorite. Thickness unknown: at least 300m. Late Permian. Geophysics modelling.||||Overlies and/or faulted against Smoky beds and Youlambie Conglomerate. Is intruded by Craiglands Quartz Monzodiorite.|Dark grey, intermediate to felsic volcanics (rhyodacites) and hypabyssal intrusives (quartz monzodiorite).|
40124|Inverness Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Yarrol Province. This unit, with the Owl Gully Volcanics and unnamed volcanic units, are all mapped under the symbol, Pvo.||||||
40124|Inverness Volcanics|68679|5|Briefly described|p312-313, p343, p425|Permian|Permian|Murray et al. (2012). Forms the eastern part of the Mount Gerard Complex of Dear et al. (1971). Northern New England Orogen. May be comagmatic with the Craiglands Quartz Monzodiorite.||||Is intruded by the Galloway Plains Igneous Complex.|Intermediate to felsic volcanics and hypabyssal intrusives; the volcanics locally exhibit fragmental textures and contain abundant small plagioclase phenocrysts; typically the groundmass is fine-grained with devitrification textures.|
78844|Iona seam package|65096|5|Briefly described|p372, p376 Fig.5, p376|Middle Jurassic|Middle Jurassic|[informal 'sequence stratigraphy' unit] Comprises a sandy package and often displays a marked change in sonic and density characteristics from the Argyle seam package. Also written as Iona seam on p372. See also fig.2, p370.||Said to be of the Juandah Coal Measures sequence.||Higher in sequence than Argyle seam package. Overlain by Wambo seam package.||
23662|Ironhurst Formation|23291|4|Described|p92 Fig. 3.9|Early Permian|Late Carboniferous|Parent: Maureen Volcanic Group. Thickness: 350-600m. Geological Province: Georgetown Region.||||||19-MAY-15
23662|Ironhurst Formation|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Maureen Volcanic Group.||||||
23662|Ironhurst Formation|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V8. I-Type.||||||
23662|Ironhurst Formation|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23662|Ironhurst Formation|40542|6|Mentioned|p97|||||||||
23662|Ironhurst Formation|43259|4|Described|Appendix 1,p1.||Carboniferous|of Maureen Volcanic Group.||||||
23662|Ironhurst Formation|43740|4|Described|p20|||Overlies Gilberton Fm, underlies Puranga Rhyolite. Includes Ant Hill Andestie Mbr, Womblealla Rhyolite Member.||||||21-SEP-04
23662|Ironhurst Formation|50595|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Maureen Volcanic Group. Includes the Womblealla Rhyolite and Ant Hill Andesite Members.||||||01-JUL-15
23662|Ironhurst Formation|68352|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Maureen Cauldron. Min Age: Early Permian?||Unit in Maureen Volcanic Group.|Includes Ant Hill Andesite Member and Womblealla Rhyolite Member.||Rhyolite, rhyolitic ignimbrite, rhyolitic volcanic, lutite arenite and rudite, andesite.|18-MAY-15
23662|Ironhurst Formation|69593|6|Mentioned|p487|||||Maureen Volcanic Group.||||
75753|Isabella Creek Rhyolite|70740|5|Briefly described|p126|Permian|Carboniferous|New unit. Of Kennedy Igneous Association.|||||Quartz-feldspar-phyric intrusive and extrusive rhyolite and microgranite.|27-MAY-20
68174|Isis Arenite|60281|5|Briefly described|Fig. 33 Appendix 1|Cretaceous|Cretaceous|Of the Maryborough Formation.  Geological Province: Maryborough Basin.||||||
29980|Ixe Suite|23291|5|Briefly described|p96 Tb. 3.11, p101 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
29980|Ixe Suite|23616|6|Mentioned|p77|||Of Ootann Supersuite||||||
29980|Ixe Suite|43060|6|Mentioned|p105|||of Ootann Supersuite||||||
41095|J P Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41095|J P Granite|65388|3|Fully described|p261-262, p236 Fig. 81, 273|Early Permian|Late Carboniferous|Interpreted to post-date Torsdale Volcanics, Wind Mill Diorite, and to pre-date the Rockdale and Moocoorooba Granites. Age uncertain. Difficult to distinguish from adjoining Rockdale Granite on geophysics. Pale grey, medium to fine-grained, uneven grained to slightly porphyritic, biotite-hornblende monzogranite. Deeply weathered.||||||
41095|J P Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age relations with several units given but contacts not observed.|||||Pale grey, medium- to fine-grained, seriate to slightly porphyritic biotite-hornblende monzogranite with common granophyric intergrowths.|
82861|J and K'' seams|73163|5|Briefly described|p467|Guadalupian|Cisuralian|Galilee Basin. Also written as combined J and K Seams. Last record of sedimentation in the Galilee Basin prior to the Lopingian. Placed at the Cisuralian-Guadalupian boundary on the basis of palynology.||Joe Joe Group||Overlying the Aramac Coal Measures with significant depositional hiatus.|Sandstone, siltstone and coal.|
27085|Jack Formation|13996|6|Mentioned|p129-132, p143, p149|Silurian|Silurian|Broken River region. The lowermost unit of this Formation has a sparse conodont fauna of Wenlock age. Higher levels contain Ludlow species. Coral assemblage. Small, undescribed trilobite fauna. Hosts acanthodian microremains, erecting a new species.||||||
27085|Jack Formation|23032|4|Described|p24 fig6|Early Devonian|Ludlow|||||||
27085|Jack Formation|23044|5|Briefly described|60|||Of Graveyard Creek Group, Broken River Province.||||||
27085|Jack Formation|23423|5|Briefly described|Plate 8.4c|||||||||
27085|Jack Formation|23424|4|Described|Table 8.1 p334.|Pridoli|Llandovery|Age: Early(?) to late Silurian (late Llandovery) to Pridoli; corals, conodonts, graptolites & trilobites. Uppermost unit of Graveyard Ck Gp. Overlies and may interfinger Poley Cow Fm. Of Graveyard Creek Gp, Graveyard Ck Subprovince. 580 m thick.||||||
27085|Jack Formation|23430|5|Briefly described|p476|||Underlain by Poley Cow Formation. Broken River Province.||||||15-APR-08
27085|Jack Formation|23431|5|Briefly described|p541|||||||||
27085|Jack Formation|23522|5|Briefly described|p250 Fig 6|Lochkovian|Silurian|||||||
27085|Jack Formation|24029|5|Briefly described|p112 Fig.1, p115 Fig.3|Llandovery|Llandovery|Of Graveyard Creek Group.||||||
27085|Jack Formation|24577|4|Described|p752 Fig. 1|Lochkovian|Silurian|Generalised strat column shows unconformably overlain by the Ralph Flint Formation; overlies the Quinton Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||06-MAY-15
27085|Jack Formation|24614|6|Mentioned|p191 Fig. 1|||Geological Province: Broken River Province. See also p206.||||||07-FEB-11
27085|Jack Formation|41260|3|Fully described|p44|||Originally Jack Limestone Member||||||
27085|Jack Formation|41679|6|Mentioned|p253|||||||||
27085|Jack Formation|41719|1|Redefined|p218|Lochkovian|Ludlow|Originally Jack Limestone Member. Ludlow to early Lochkovian.||||||
27085|Jack Formation|41739|6|Mentioned|Fig.2|||||||||
27085|Jack Formation|42031|5|Briefly described|p760|||||||||
27085|Jack Formation|42054|6|Mentioned|p273|||||||||
27085|Jack Formation|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27085|Jack Formation|42709|6|Mentioned|map legend|||||||||
27085|Jack Formation|42933|1|Redefined|p65|Early Devonian|Late Silurian|Of Graveyard Creek Group. Supersedes Jack Limestone Member.||||||15-APR-08
27085|Jack Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Graveyard Creek Group.||||||
27085|Jack Formation|50088|5|Briefly described|p472|Silurian|Silurian|Contains conodonts - in the Broken River region.||||||
27085|Jack Formation|50093|6|Mentioned|p330 Fig.3 |||||||||07-FEB-11
27085|Jack Formation|50096|5|Briefly described|p75|Early Devonian|Ludlow|Of the Graveyard Creek Group. Ozarkodina conodonts found.||||||09-MAR-05
27085|Jack Formation|60332|6|Mentioned|p952|||Contains Belodella anomalis (conodont).||||||
27085|Jack Formation|61892|6|Mentioned|p229|||Northern Qld. Conodont mentioned.||||||
27085|Jack Formation|61894|5|Briefly described|p182|Late Silurian|Late Silurian|Broken River area.  Contains Pseudoplasmopora sp.B. Appears on the same page as Jack Limestone Member (of Graveyard Creek Formation).||Graveyard Creek Group.|||Contains fossiliferous limestone lenses.|
27085|Jack Formation|65214|6|Mentioned|p272|Devonian|Devonian|QLD NORTH and Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27085|Jack Formation|66498|6|Mentioned|p39-41|Ludlow|Ludlow|Broken River region, north Queensland.||||||
27085|Jack Formation|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince. Two un-named facies are mapped separately: limestone, mainly calcilutite and fine-grained pelloidal limestone, local oncolitic/oolitic limestone and coralline limestone and mudstone; coarse-grained quartzose sandstone to conglomerate.||Unit in Graveyard Creek Group.|||Micaceous, quartzose to sublabile sandstone and mudstone, locally fossiliferous; limestone and coarse-grained quartzose sandstone and conglomerate.|
27085|Jack Formation|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince. Two un-named facies are mapped separately: limestone, mainly calcilutite and fine-grained pelloidal limestone, local oncolitic/oolitic limestone and coralline limestone and mudstone; coarse-grained quartzose sandstone to conglomerate.||Unit in Graveyard Creek Group.|||Micaceous, quartzose to sublabile sandstone and mudstone, locally fossiliferous; limestone and coarse-grained quartzose sandstone and conglomerate.|
27085|Jack Formation|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince.||Of the Graveyard Creek Group.||Conformably underlain by the Poley Cow Formation.|Micaceous, quartzose to sublabile sandstone and mudstone, locally fossiliferous; minor limestone and coarse-grained quartzose sandstone and conglomerate.|
27085|Jack Formation|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince.||Of the Graveyard Creek Group.||Conformably underlain by the Poley Cow Formation.|Micaceous, quartzose to sublabile sandstone and mudstone, locally fossiliferous; minor limestone and coarse-grained quartzose sandstone and conglomerate.|
27085|Jack Formation|69030|5|Briefly described|p6|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province).||Graveyard Creek Group||||
27085|Jack Formation|69592|3|Fully described|p259, p261-263, p267|Lochkovian|Wenlock|Graveyard Creek Subprovince, Broken River Province. Forms the Jack Hills where the 580m-thick type section is in the eponymous Gorge cut by the Broken River (Withnall, 1989; Withnall et al., 1993). Raised to Group status by Jeppson et al. (2007), thereby elevating the Graveyard Creek Group to Supergroup; the four formations were not formally defined; they are regarded here as informal members. Fence diagram; unit thins to E and S. The oncolitoc/oolitic limestone unit is rich in corals and is known as the "coral gardens". Shallow shelf deposits. Diverse fauna with Wenlock conodonts. Appears on p263 also as Jack Limestone.||Graveyard Creek Group.||Conformably overlies (possibly interfingers with) Poley Cow Formation (=Quinton Formation). Is overlain by Ralph Flint Formation, Shield Creek Formation and Burges Formation (Broken River Group).|Basal massive, thick-bedded lime mudstone, partly dolomitised, overlain by thick-bedded, medium- to coarse-grained, micaceous quartz sandstone, shale and minor limestone lenses, then oncolitic and oolitic limestone beds, and massive lime mudstone.|
27085|Jack Formation|73143|6|Mentioned|p9|Early Devonian|Late Silurian|Contains conodonts, Cypricriodus hesperius from upper limestone unit (Simpson, 1998, 2000) reassigned to Praeicriodus simpsoni by Murphy et al., (2016) with a latest Silurian age instead of early Devonian.|||||Includes limestone units.|
73024|Jack Hills Limestone|63152|5|Briefly described|p120 Fig. 3|||Of the Jack Group (Graveyard Creek Supergroup). Overlies Coral Gardens Formation. Massively bedded limestone overlying oncolitic and oolitic limestones below.||||||10-APR-07
77840|Jack Shay Gabbro|65388|2|Defined|p321-322, 257,  p301 Fig 98|Early Triassic|Late Permian|Previously mapped as part of Delubra Quartz Gabbro. Crops out along eastern margin of Glisson Granodiorite. Probably intrudes it. Intrudes Yerilla Metamorphics, Narayen beds. K-Ar (hornblende) age: 251+/-7Ma. Appears to be a composite body based on both geophysics and field observations. The southern part appears to be olivine gabbro. ||||||
77840|Jack Shay Gabbro|68679|5|Briefly described|p418-419|||Southern part of the Rawbelle Batholith. ~30 km2.|251 +/- 7 Ma (K-Ar: Whitaker et al., 1974).|||Intrudes Yerilla Metamorphics, Narayen beds, and ?Glissons Granodiorite or ?Evandale Tonalite.|Layered, pyroxene-hornblende quartz gabbro and gabbro.|
72734|Jackass Gabbro|65452|6|Mentioned|p6 Fig.2|Permian|Permian|||||||
72734|Jackass Gabbro|67203|6|Mentioned|p6|Permian|Permian|||||||
72734|Jackass Gabbro|68008|5|Briefly described|p324, p326, p414|||Miriam Vale 100k sheet. Appears to be equivalent to the Miriam Vale Granodiorite.||||Is intruded by Bororen Tonalite.||
72734|Jackass Gabbro|68319|5|Briefly described|Map Legend|Permian|Permian||||||Dark grey, fine to medium-grained, hornblende-clinopyroxene gabbro to diorite; locally with minor orthopyroxene, biotite, quartz; commonly partly altered; minor granodiorite.|
72734|Jackass Gabbro|68679|5|Briefly described|p337, p410, p421-423|||Gayndah-Gladstone belt, northern New England Orogen.|268.3 +/- 1.7 Ma (SHRIMP: Cross et al., 2012).|||Adjacent to and intimately associated with Many Peaks Granite.|Clearly composite: hornblende-clinopyroxene gabbro to diorite; minor granodiorite. Minor orthopyroxene, biotite.|
72734|Jackass Gabbro|73450|6|Mentioned|p7, p9|late Permian|late Permian|||||Intruded by Foreshores Granite and Castletower Granite.||
22010|Jacks Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite.||||||
22010|Jacks Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
22010|Jacks Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 438. I-Type.||||||
22010|Jacks Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22010|Jacks Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
22010|Jacks Granite|43087|2|Defined|p56|Late Carboniferous||Supersedes Brooklands Granite of Richards (1981).||||||
22010|Jacks Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22010|Jacks Granite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
22010|Jacks Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Comprises five subunits of biotite leucogranite, biotite leucogranite and aplite, to biotite granite - detailed lithology included in Appendix, p278-9.||||||07-FEB-11
22010|Jacks Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Five variants are mapped separately.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Mainly pink to grey, fine- to coarse-grained, usually porphyritic, biotite granites and biotite leucogranites; locally aplitic.|
36432|Jacobsens Track Granodiorite|23422|5|Briefly described|p182|||See also Jacobsens Creek Granodiorite.||||||
36432|Jacobsens Track Granodiorite|23617|3|Fully described|Table 2 p16||Early Permian|286 Ma (K-Ar). Also see p33. Intrudes Running River Metamorphics + Falls Creek Tonalite. Unit forms an oval pluton in the headwaters of Flagstone Creek. Also Table 3 p52. Kennedy Province.||||||
36432|Jacobsens Track Granodiorite|23618|5|Briefly described|map legend||Early Permian|||||||
36432|Jacobsens Track Granodiorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
22015|James Creek Granite|23423|5|Briefly described|p305 Table 7.4|||Yongala Volcanic Subgroup unconformably overlies.||||||21-AUG-15
22015|James Creek Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 291+/-6 Ma, 299 Ma,  Rb-Sr. Ootann Supersuite.||||||
22015|James Creek Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite. Age: ~299Ma.||||||
22015|James Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 274. I-Type.||||||
22015|James Creek Granite|23616|6|Mentioned|Table 3 p47|||||||||
22015|James Creek Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).  Pale to medium grey or pinkish grey, medium to coarse biotite granite; variably altered.Age: 299Ma.||||||15-JUN-06
22015|James Creek Granite|43259|4|Described|Appendix 1,p35.||Late Carboniferous|Age is 299 Ma.||||||
22015|James Creek Granite|43567|5|Briefly described|Table 2,p401|||||||||
22015|James Creek Granite|43626|6|Mentioned|p10||Late Carboniferous|"Wolfram"||||||
22015|James Creek Granite|60425|4|Described|p49 Tb.3, p189, p278-9 Appdx.|Early Permian|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Age: 291+/-6Ma, 299Ma (Rb-Sr). Intruded Hodgkinson Fm. Overlain by Beapeo Rhyolite (Featherbed Volcanic Gp). Hosts the Wolfram Camp molybdenum-tungsten-bismuth deposit. Detailed lithology included (p278-9 Appdx.). I-type.||||||30-MAR-15
22015|James Creek Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The five sub-units are mapped separately. Other dating gives ages of 299 Ma (Rb-Sr, plagioclase) and 303 Ma (Rb-Sr, muscovite). Lithology note continued - a geophysical subdivision variant on the last unit.|297 +/- 6 Ma (Rb-Sr, total rock).|Unit in Ootann Supersuite.|||Porphyritic biotite granite with numerous enclaves to several metres across; fine- to coarse-grained biotite granite and leucogranite, variably altered; extensively mineralised biotite granite; pink biotite leucogranite.|25-MAR-15
22016|Jamtin Rhyolite|23291|5|Briefly described|p37|||Parent: Featherbed Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
22016|Jamtin Rhyolite|23423|4|Described|p306 Table 7.3||Late Carboniferous|Age: 301 +/- 11 Ma (Rb-Sr). Extensively intruded by granites of the Ootann and Almaden Supersuites. Featherbed Volcanic Group. Underlying unit Chillagoe Formation (unconformable).||||||
22016|Jamtin Rhyolite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Featherbed Volcanic Group, Kennedy Province.||||||
22016|Jamtin Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 301+/-11Ma Rb-Sr. of Featherbed Volcanic Group.||||||02-APR-15
22016|Jamtin Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V122. I-Type.||||||
22016|Jamtin Rhyolite|23616|5|Briefly described|Table 3 p50||Late Carboniferous|Age: 301+/-11 Ma (Rb-Sr). Unconformable on the Chillagoe Fm; extensively intruded by granites of Almaden & Ootann Supersuites and by rhyolite dykes. Of Featherbed Volcanic Gp.||||||
22016|Jamtin Rhyolite|23713|5|Briefly described|p24||Late Carboniferous|||||||
22016|Jamtin Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group||||||
22016|Jamtin Rhyolite|43083|5|Briefly described|p91|||Of Featherbed Volcanic Group. Age: 301+/-11 Ma. (Rb-Sr). Rhyolitic and dacitic ignimbrites. Intruded by Almaden and Ruddygore Granodiorites, by Pinchgut and Retchford Granites and also by Lags Microgranite.||||||02-APR-15
22016|Jamtin Rhyolite|43087|5|Briefly described|p55|||Rb-Sr biotite age of 301+/-11 Ma. Of Featherbed Volcanic Group.||||||
22016|Jamtin Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group. Leucocratic rhyolitic ignimbrite. Age: 301+/-11Ma.||||||02-APR-15
22016|Jamtin Rhyolite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|of Featherbed Volcanic Group. The age is 301+/-11 Ma.||||||
22016|Jamtin Rhyolite|43567|6|Mentioned|Fig.2,p398||Late Carboniferous|||||||
22016|Jamtin Rhyolite|43626|2|Defined|p10,39||Late Carboniferous|Minimum age: 301+/-11 Ma (L.D.Black, AGSO, 1993)(Minimum age). May have been reset by intrusion of Almaden Granite.||||||17-AUG-15
22016|Jamtin Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22016|Jamtin Rhyolite|60425|4|Described|p48 Tb. 3|||Of Featherbed Volcanic Group. Comprises 6 informal units. Unconformable on Chillagoe Fm. Extensively intruded by Almaden and Ootann Supersuite granites. Age: 301+/-11Ma (Rb-Sr). Welded, crystal-poor to crystal-rich dacitic to rhyolitic ignimbrite.||||||07-FEB-11
22016|Jamtin Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Seven facies are mapped separately.||Unit in Featherbed Volcanic Group.|||Rhyolitic and dacitic ignimbrites.|
22016|Jamtin Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|301 Ma.|Featherbed Volcanic Group.||||
41097|Jan Mar Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41097|Jan Mar Granite|65388|4|Described|p260, p236 Fig. 81|Early Permian|Late Carboniferous|Intrudes Torsdale Volcanics. Interpreted to pre-date parts of Camboon Volcanics. Age tentative. Mainly white to pale brown, or red (extensively weathered), medium-grained, even-grained to slightly porphyritic, leucocratic biotite monzogranite.||||||
41097|Jan Mar Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Predates Camboon Volcanics.||||Intrudes Torsdale Volcanics.|Medium-grained, equigranular to slightly porphyritic, leucocratic biotite monzogranite.|
36646|Janet Ranges Volcanic Group|23420|4|Described|p 146 table 4.5|Early Permian|Late Carboniferous|Also see p 129. I-type characteristics. Overlies Sefton Metamorphics. Intruded by Weymouth Granite.||||||20-JUN-12
36646|Janet Ranges Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Elimeek and Wallaman Falls Volcanics; Koolmoon, Silent Creek and Torres Strait Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
36646|Janet Ranges Volcanic Group|69593|5|Briefly described|p475-477|||Northern Coen region. Crops out over ~375 km2. 300-500m thick. Rhyolitic-dacitic rocks of this unit are tentatively included in the Weymouth Supersuite. Age from an intrusive constituent.|285 +/- 9 Ma.||||Rhyolitic ignimbrite, tuff, lava and breccia; some andesite, dacite and rhyodacite.|
36646|Janet Ranges Volcanic Group|71031|6|Mentioned|p3, p43|Early Permian|Early Permian|Coen region. Previously correlated tentatively with the Torres Strait Volcanic Group.||||||
36646|Janet Ranges Volcanic Group|71792|5|Briefly described|p22, p34||||||Includes the Janet Ranges Volcanics, Kangaroo River Volcanics|||
36646|Janet Ranges Volcanic Group|71853|5|Briefly described|Map legend.|Permian|Permian||||Janet Ranges Volcanics, Kangaroo River Volcanics.|||
36646|Janet Ranges Volcanic Group|72983|4|Described|p4, p7, p60, p66-69|Kungurian|Artinskian|Jardine Subprovince, Kennedy Igneous Association. Coen Inlier, northwestern. Cape York region. Date is a crystallisation age from a rhyolitic ignimbrite (sample 2306987/DPCY001). Strong temporal relationship with the Weymouth Granite.|284.7 +/- 1.7 Ma SHRIMP U-Pb|||Intruded by Weymouth Granite. Underlain by Pascoe River beds.|Rhyolitic ignimbrites, coherent and autoclastic rhyolitic lavas and subvolcanic intrusions.|
36308|Jape Creek Granodiorite|23510|5|Briefly described|Map Legend||Silurian|of White Springs Supersuite.||||||
36308|Jape Creek Granodiorite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
36345|Jasmin Granite|22461|5|Briefly described|p473|||||||||
26308|Jayah Creek Metabasalt|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
26308|Jayah Creek Metabasalt|24419|5|Briefly described|p16, p12 Fig. 4, p13 Fig. 5|Proterozoic|Proterozoic|Of Haslingden Gp. Includes Timothy Creek Sst Mbr (main sedimentary unit). Basalt lava flows with mainly arenaceous sedimentary intercalations.   Unconformably overlies Saint Ronans Metamorphics, Kallala Quartzite and Sulieman Gneiss.  See also p15 Fig. 6.||||||
26308|Jayah Creek Metabasalt|37862|4|Described|p587|||||||||
26308|Jayah Creek Metabasalt|38234|4|Described|p103|||||||||
26308|Jayah Creek Metabasalt|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Timothy Creek Sandstone Member.||||||25-AUG-04
26308|Jayah Creek Metabasalt|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26308|Jayah Creek Metabasalt|38658|6|Mentioned|p152|||||||||
26308|Jayah Creek Metabasalt|39445|5|Briefly described|Table 2|||||||||
26308|Jayah Creek Metabasalt|39622|6|Mentioned|p19|||||||||
26308|Jayah Creek Metabasalt|40840|6|Mentioned|Map legend|||||||||
26308|Jayah Creek Metabasalt|41978|6|Mentioned|p497|||||||||
26308|Jayah Creek Metabasalt|42565|4|Described|Table 1 p6|||||||||15-MAR-18
26308|Jayah Creek Metabasalt|43928|6|Mentioned|23|||||||||
26308|Jayah Creek Metabasalt|45161|4|Described|p11|||||||||
26308|Jayah Creek Metabasalt|45166|4|Described|p16|||||||||
26308|Jayah Creek Metabasalt|49009|2|Defined|p17|Precambrian|Precambrian|Mapped as Eastern Creek Volcs. Noakes & others 1959. See also p48.||||||15-MAR-18
26308|Jayah Creek Metabasalt|49041|5|Briefly described|Table 1|||||||||
26308|Jayah Creek Metabasalt|50536|6|Mentioned|p4.1|||Geological Province: Mount Isa Inlier.||||||
26308|Jayah Creek Metabasalt|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metabasalt, amphibolite, schist, quartzite, meta-arenite.||||||
26308|Jayah Creek Metabasalt|64250|6|Mentioned|p11 fig.3|||Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||14-MAR-18
26308|Jayah Creek Metabasalt|65387|6|Mentioned|p55-56|||Intruded by unnamed gneissic granite with 1782 +/-5 Ma U/Pb zircon SHRIMP age interpreted as magmatic crystallisation age.||||Equated with Eastern Creek Volcanics.|Includes sandstone.|04-APR-18
26308|Jayah Creek Metabasalt|65396|6|Mentioned|p82, p175|Statherian|Statherian|Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform.||||||
26308|Jayah Creek Metabasalt|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Leichhardt Superbasin.||Lower Haslingden Group.|||Amphibolitic metabasalt; numerous metasedimentary intercalations.|
26308|Jayah Creek Metabasalt|67539|6|Mentioned|p9 Fig.7|||||||||
26308|Jayah Creek Metabasalt|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence.||Haslingden Group.|||Amphibolitic metabasalt; numerous metasedimentary intercalations.|
26308|Jayah Creek Metabasalt|73083|6|Mentioned|p70, p72|||||||||
26308|Jayah Creek Metabasalt|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Mafic extrusives, includes minor siliciclastics.|
31677|Jedda Schist|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
31677|Jedda Schist|43596|4|Described|p12, p21 Tb. 1||Proterozoic|Of Yambo Metamorphic Gp. Faulted against Saraga Schist in W. Intruded by Cape York Peninsula Batholith. Geol.prov: margin of Yambo Inlier. Two subunits - a two-mica schist with thin psammitic schist interbeds, + a mylonitised granitoid. Incl. lith detail.||||||07-APR-15
31677|Jedda Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Yambo Metamorphic Group||||||
31677|Jedda Schist|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Is intruded by the Cape York Peninsula Batholith.||Yambo Metamorphic Group.||Faulted against Saraga Schist.|Two-mica(+/- garnet) granitic to granodioritic mylonite; and two-mica schist, psammitic schist.|
25962|Jericho Formation|13516|5|Briefly described|p147, fig 5|Early Permian|Late Carboniferous|From Galilee Basin|||Includes Oakleigh Siltstone Member|||
25962|Jericho Formation|23430|4|Described|p519 Table 14.6|||Maximum thickness <760 m||||||
25962|Jericho Formation|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
25962|Jericho Formation|30916|6|Mentioned|p99|||||||||
25962|Jericho Formation|31120|6|Mentioned|p148|||See also P149||||||
25962|Jericho Formation|31121|6|Mentioned|p385|||||||||
25962|Jericho Formation|31122|2|Defined|p349|Early Permian|Late Carboniferous|Probably Late Carboniferous to Early Permian||||||
25962|Jericho Formation|31258|4|Described|p100|||re  petroleum prospects||||||
25962|Jericho Formation|31860|6|Mentioned|p277|||See also P280||||||
25962|Jericho Formation|32138|6|Mentioned|p397|||||||||
25962|Jericho Formation|33372|5|Briefly described|p16|||See also P24. From wells.||||||
25962|Jericho Formation|33674|4|Described|p438|||Lithology.||||||
25962|Jericho Formation|35457|6|Mentioned|p627|||Also Fig.4 biostratigraphic relationships.||||||
25962|Jericho Formation|35845|6|Mentioned|Fig.25|||||||||
25962|Jericho Formation|36243|6|Mentioned|Table 5A|||||||||
25962|Jericho Formation|36562|6|Mentioned|p547|||||||||
25962|Jericho Formation|36921|4|Described|p183|||See also Table 1.||||||
25962|Jericho Formation|37451|6|Mentioned|Table 2|||||||||
25962|Jericho Formation|37610|3|Fully described|p301|||See also Fig.3.||||||
25962|Jericho Formation|39252|6|Mentioned|p13|||||||||
25962|Jericho Formation|39261|6|Mentioned|Fig. 9|||||||||
25962|Jericho Formation|39264|6|Mentioned|Fig. 13|||||||||
25962|Jericho Formation|39265|6|Mentioned|Fig. 3|||||||||
25962|Jericho Formation|39445|5|Briefly described|Table 7|||||||||
25962|Jericho Formation|39478|6|Mentioned|Table 1|||||||||
25962|Jericho Formation|39847|6|Mentioned|p34|||||||||
25962|Jericho Formation|39943|6|Mentioned|Table 7A|||||||||
25962|Jericho Formation|39989|6|Mentioned|p426|||||||||
25962|Jericho Formation|39991|6|Mentioned|p428|||||||||
25962|Jericho Formation|40123|6|Mentioned|p465|||||||||
25962|Jericho Formation|41116|4|Described|p430|||||||||
25962|Jericho Formation|41198|6|Mentioned|Table 1|||||||||
25962|Jericho Formation|41270|6|Mentioned|p278|||||||||
25962|Jericho Formation|41707|6|Mentioned|p166|||||||||
25962|Jericho Formation|41710|6|Mentioned|Fig.2|||||||||
25962|Jericho Formation|42446|6|Mentioned|p15|||||||||
25962|Jericho Formation|42447|6|Mentioned|Fig.3|||||||||
25962|Jericho Formation|42491|6|Mentioned|p5|||||||||
25962|Jericho Formation|42547|4|Described|p80|||||||||
25962|Jericho Formation|42999|5|Briefly described|p95,Table1,p90|||||||||
25962|Jericho Formation|43105|5|Briefly described|p13|||||||||
25962|Jericho Formation|43114|6|Mentioned|p17|||||||||
25962|Jericho Formation|43812|6|Mentioned|Fig.3,p145|||||||||
25962|Jericho Formation|46849|6|Mentioned|Fig. 7|||||||||
25962|Jericho Formation|63713|5|Briefly described|p1505, p1507 Fig.2, p1508|Permian|Pennsylvanian|Glaciogenic sediments.||Unit in Joe Joe Group.||Overlies Lake Galilee Sandstone. Is overlain by Jochmus Formation.||
25962|Jericho Formation|64288|4|Described|p531-556    |Moscovian|Serpukhovian|Deposited during the mid-Namurian to early Stephanian. Contains the only unequivocal evidence of a Namurian/Westphalian glaciation outside South America: it preserves a suite of proglacial to terminal glacial facies from three separate glacial advances. Detailed sedimentology.||Of the Joe Joe Group.||Overlies Lake Galilee Sandstone. Is overlain by Jochmus Formation.|Massive and stratified diamictites, laminated siltstones with outsized clasts and interlaminated siltstone/conglomerate and sedimentary dykes and breccias.|
25962|Jericho Formation|65489|6|Mentioned|p144 Fig.53|Permian|Late Carboniferous|Koburra Trough, Galilee Basin.||||||
25962|Jericho Formation|66188|6|Mentioned|435, 437, 441, Fig 3, TB1, Fig 16-17|Early Permian|Late Carboniferous|Includes the Oakleigh and Lake Galilee Sandstone for the purposes of this study.||||||
25962|Jericho Formation|67402|5|Briefly described|p124 fig GLL1|Sakmarian|Asselian|Galilee Basin. Deposited in a low energy fluvial environment. Generally has fair reservoir qualities that degrades rapidly with depth. See also p125 tbl GLL1, p128 fig GLL8, p129 fig GLL9, p131 fig GLL12, p132, p135, p136, p137.  |||Includes the Oakleigh Siltstone Member.|Overlies the Lake Galilee Sandstone. Overlain by the Jochmus Formation.|Mudstone and siltstone with subordinate quartz and lithic-rich sandstone.|
25962|Jericho Formation|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-8|Kasimovian|Bashkirian|Hawkins (1978). Galilee Basin.||Unit in Joe Joe Group.|Includes Oakleigh Siltstone Member.|Is overlain by Jochmus Formation.|Interbedded mudstones containing small amounts of illite-smectite mixed layers, siltstones, and sandstones which consist mainly of quartz and lithic fragments.|
25962|Jericho Formation|68413|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Galilee Basin? Early Permian minimum age.||||Conformably overlain by the Jochmus Formation.|Mudstone, siltstone, sandstone.|
25962|Jericho Formation|68731|6|Mentioned|p198, p201 Fig 3.110, p203|Pennnsylvanian|Pennnsylvanian|||Of the Joe Joe Group.|Includes the Oakleigh Siltstone Member.|||
25962|Jericho Formation|69582|6|Mentioned|p65-p66|Late Carboniferous|Late Carboniferous|Galilee Basin. Intersected in GSQ Longreach 2 drillhole.||||Unconformably overlies the Lake Galilee Sandstone. Overlain by the Jochmus Formation.|Sandstone.|
25962|Jericho Formation|71265|5|Briefly described|p589|Kasimovian|Bashkirian|Galilee Basin.||Joe Joe Group.|Oakleigh Siltstone Member.|Overlies Lake Galilee Sandstone. Is overlain by Jochmus Formation.||
25962|Jericho Formation|71701|4|Described|p155-p156|Kasimovian|Bashkirian|Koburra Trough, Powell Depression and Springsure Shelf, Galilee Basin.||Joe Joe Group|Includes the Oakleigh Siltstone Member.|Overlies the Lake Galilee Sandstone. Overlain by the Jochmus Formation.||08-FEB-23
25962|Jericho Formation|71710|5|Briefly described|p377, p378 Fig 13, p381, p384-386|||Galilee Basin. See also: Upper Jericho Formation and Lower Jericho Formation. Depositional environment and sequence stratigraphy is described.||Of Joe Joe Group. Lower part included in sequence 1, this paper.|Informally subdivided into lower and upper parts, with Oakleigh Siltstone Member between.|Overlies Lake Galilee Sandstone. Unconformably overlain by Jochmus Formation.||
25962|Jericho Formation|72088|4|Described|p8, p17, p91|Moscovian|Serpukhovian|Northeastern and southern Galilee Basin. Deposited in a fluvio-lacustrine environment. Local dropstones and pebbly mudstones indicate a glacial influence.||Joe Joe Group|Includes the Oakleigh Siltstone Member.|Conformably overlies the Lake Galilee Sandstone. Overlain by the Jochmus Formation.|Mudstone, siltstone and volcaniclastic sandstone.|
25962|Jericho Formation|73163|5|Briefly described|p467|Asselian|Pennsylvanian|Galilee Basin. Widespread. Deposited in an active extensional basin. 1992 reference on p467 to the Jericho Formation being Pennsylvanian (Jones and Truswell, 1992), but is a part of the Joe Joe Group described as Cisuralian in age.||Joe Joe Group|Oakleigh Siltstone Member|Conformably overlying Lake Galilee Sandstone. Underlying the Jochmus Formation.|Characterised by glacial sedimentary structures. Includes series of interbedded siltstones, mudstones, and shales in upper part.|
25962|Jericho Formation|73472|6|Mentioned|p115-116|Kasimovian|Bashkinian|Galilee Basin.||Joe Joe Group|Oakleigh Siltstone Member|Underlain by Lake Galilee Sandstone. Overlain by Jochmus Formation. Equivalent to Boonderoo beds.||
34691|Jessop Creek Tonalite|22847|3|Fully described|p 56|Middle Devonian|Early Devonian|||||||
34691|Jessop Creek Tonalite|23083|6|Mentioned|Fig 1 p679, p681|||||||||
34691|Jessop Creek Tonalite|23422|5|Briefly described|p213 Table 6.8|||||||||
34691|Jessop Creek Tonalite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
34691|Jessop Creek Tonalite|23513|5|Briefly described|Map legend||Devonian|Palaeozoic Intrusive No. 193. I-Type.||||||
34691|Jessop Creek Tonalite|43936|5|Briefly described|Map legend|Devonian|Silurian|||||||
34691|Jessop Creek Tonalite|62075|6|Mentioned|p15 Fig.7|Early Devonian|Early Devonian|Ravenswood batholith. Appears as Jessop Creek tonalite.||||||
74030|Jibbinbar Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|White to pale brown, pale grey, or brown to reddish brown, fine- to medium-grained, mainly even-grained (allanite-titanite-)biotite syenogranite; commonly altered.||||||
74030|Jibbinbar Granite|63748|4|Described|p30-31|||In the Mount You You Suite. Intrudes Texas beds. Mainly white to pale brown, pale grey, or brown to reddish-brown, fine- to medium-grained, even-grained biotite syenogranite. See also p27 Fig.27||||||07-FEB-11
74030|Jibbinbar Granite|65668|5|Briefly described|p1, p2 Tb.1, p16-18|Permian|Permian|Stanthorpe area; New England Orogen. Formerly of the Ruby Creek Granite (Olgers, 1974). Redefined (Donchak et al., 2007) on age, geochemical and mineralogical grounds as part of Mount You You Supersuite. Age 298.1 +/- 2 Ma (SHRIMP U-Pb zircon). Buff, fine-medium grained altered leucocratic biotite syenogranite.||||||
74030|Jibbinbar Granite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Mount Bullaganang, Mount You You and Palgrave Granites; Boxwell and Greymare Granodiorites; are all mapped under the symbol, Pgn.||||||
74030|Jibbinbar Granite|68679|5|Briefly described|p445, p454-457, p466|Permian|Permian|Northern New England Batholith. ~7 km2. The oldest of several small leucogranite stocks. Had been mapped as Ruby Creek Granite (Robertson, 1974); differences listed. Appears as Jibbenbar Granite on p445. Associated with As mineralisation in quartz veins and lodes, with erratic Au values.|298.1 +/- 2.0 Ma (SHRIMP: Cross et al., 2009).|Mount You You Suite.|||Fine- to medium-grained, mainly even-grained, leucocratic biotite syenogranite; texturally heterogeneous; common granophyric intergrowths; enclaves of country rock near contact. Reduced, moderately-highly evolved, high-K, I-type.|
74030|Jibbinbar Granite|68901|5|Briefly described|p8, p6|Early Permian|Early Permian|New England Region. SHRIMP age derived from Cross et al, 2009.|298.1 +/- 2 Ma (SHRIMP U-Pb)|||||26-SEP-18
74030|Jibbinbar Granite|69639|5|Briefly described|p44, p220|Asselian|Gzhelian|New England Orogen.|298.1 +/- 2 Ma (Cross et al, 2009)|Mount You You Supersuite||||
74030|Jibbinbar Granite|70373|6|Mentioned|p790, p804|Early Permian|Late Carboniferous|Texas Orocline area.|~298 Ma||||S type granitoids.|
74030|Jibbinbar Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|298+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
74030|Jibbinbar Granite|71628|5|Briefly described|p5: 1|||Donchak et al. (2007). Now Jibbinbar Leucosyenogranite.||Mount You You Suite.||||
74030|Jibbinbar Granite|73202|6|Mentioned|p637|Asselian|Gzhelian|Anaiwan terrane (also spelt Anawian), western. I-type plutonism.|298.1 +/- 2 Ma|||||
82508|Jibbinbar Leucosyenogranite|71628|4|Described|p5: 1-4, 8-9; p19:150|Permian|Permian|Originally the Jibbinbar Granite (Donchak et al., 2007); the name is changed (?in this study) to reflect the dominant lithology. Named after the parish of Jibbinbar or Mount Jibbinbar where the unit crops out prominently. Occurs ~30 km SW of Stanthorpe; forms pavements, prominent bare rock outcrops, and numerous boulders. Geochemistry described. Associated with significant As (-Au, Ag) mineralisation: probably metahydrothemal rather than granite-related in origin.|298.1 +/- 2.0 Ma (SHRIMP: Cross et al., 2009).|Mount You You Suite.||Intrudes the Texas beds.|White to pale brown, pale grey, or brown to reddish brown; fine- to medium-grained, typically even-grained but locally porphyritic, biotite syenogranite; commonly altered. I-type.|
29599|Jimna Phyllite|22845|2|Defined|p7,9,11,36-9,69,76,7|Early Carboniferous|Late Devonian|Mapped by Murphy (1976) as Bunya Phyllite, new name after Sliwa (1994)||||||
29599|Jimna Phyllite|22846|6|Mentioned|p44,47|Carboniferous|Devonian|Intruded by Neurum Complex.||||||
29599|Jimna Phyllite|23799|5|Briefly described|p126|||Polydeformed basement rocks. Overlain by Marumba beds. Geological Province: Yarrol Province.||||||27-OCT-08
29599|Jimna Phyllite|43588|6|Mentioned|p30||Late Devonian|||||||
29599|Jimna Phyllite|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
29599|Jimna Phyllite|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince. Polydeformed slate and phyllite with scattered meta-chert layers; foliated mafic greenschist.||||||
29599|Jimna Phyllite|61782|5|Briefly described|p277 Fig. 3|||Unconformably overlain by Marumba Beds. Geological Provience: Esk Trough.||||||
29599|Jimna Phyllite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
29599|Jimna Phyllite|68679|5|Briefly described|p321, p326-327, p330-331, p386|Paleozoic|Paleozoic|Sliwa (1994). Previously mapped as Bunya Phyllite by Murphy et al. (1976), and later assigned to the Booloumba beds by Murray et al. (1979). North D'Aguilar Subprovince, northern New England Orogen. Crops out over 373 km2, S of Jimna. Detachment zone and lower plate accretionary assemblages. Is equivalent to Anderson Creek and Bunya Phyllites.||||Is faulted against the Rocksberg and Peters Creek Greenstones, and Marumba, Northbrook and Booloumba beds. Is intruded by Neurum Complex and Tungi Creek Granodiorite.|An assemblage of low-grade, polydeformed phyllite, slate, metachert, and lenses (to 4km long) of massive to strongly foliated mafic greenschist. Has a distinct micaceous sheen on cleavage surfaces. Contains thin lenses of very fine-grained quartzite.|
28230|Joe Joe Group|13516|6|Mentioned|p147, fig 5|Early Permian|Late Carboniferous|From Galilee Basin||||||
28230|Joe Joe Group|22800|6|Mentioned|Fig.7 p586|Early Permian|Late Carboniferous|||||||
28230|Joe Joe Group|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
28230|Joe Joe Group|30915|6|Mentioned|p99|||||||||
28230|Joe Joe Group|30916|6|Mentioned|p99|||||||||
28230|Joe Joe Group|31120|4|Described|p148|||||||||
28230|Joe Joe Group|31121|6|Mentioned|p385|||||||||
28230|Joe Joe Group|31122|2|Defined|p344|Early Permian|Early Carboniferous|Late Carboniferous - Early Permian||||||
28230|Joe Joe Group|31258|5|Briefly described|p98|||||||||
28230|Joe Joe Group|31860|6|Mentioned|p277|||||||||
28230|Joe Joe Group|32138|6|Mentioned|p397|||||||||
28230|Joe Joe Group|32639|6|Mentioned|p76|||||||||
28230|Joe Joe Group|33372|6|Mentioned|p16|||Strat.||||||
28230|Joe Joe Group|33674|6|Mentioned|p438|||||||||
28230|Joe Joe Group|35457|4|Described|p627|||Also Fig.4 biostratigraphic relationships.||||||
28230|Joe Joe Group|35811|6|Mentioned|p565|||||||||
28230|Joe Joe Group|36045|6|Mentioned|p328|||||||||
28230|Joe Joe Group|36562|6|Mentioned|p547|||||||||
28230|Joe Joe Group|36596|6|Mentioned|Text Fig.2|||||||||10-FEB-06
28230|Joe Joe Group|36739|6|Mentioned|p4|||See also P21.||||||
28230|Joe Joe Group|36921|6|Mentioned|p174|||See also Table 1.||||||
28230|Joe Joe Group|37565|6|Mentioned|Fig.8|||||||||
28230|Joe Joe Group|37610|4|Described|p301|||||||||
28230|Joe Joe Group|39252|6|Mentioned|p13|||||||||
28230|Joe Joe Group|39264|6|Mentioned|Fig.1|||||||||
28230|Joe Joe Group|39266|6|Mentioned|p226|||||||||
28230|Joe Joe Group|39273|6|Mentioned|Fig. 7|||||||||
28230|Joe Joe Group|39445|5|Briefly described|p94|||Gas & oil. See also P92 & Table 7||||||
28230|Joe Joe Group|39478|6|Mentioned|Table 1|||||||||
28230|Joe Joe Group|39847|6|Mentioned|p34|||||||||
28230|Joe Joe Group|39989|6|Mentioned|p426|||||||||
28230|Joe Joe Group|39994|6|Mentioned|p200|||||||||
28230|Joe Joe Group|40623|5|Briefly described|p80|||||||||
28230|Joe Joe Group|41116|5|Briefly described|Table 1|||||||||
28230|Joe Joe Group|41198|6|Mentioned|Table 1|||||||||
28230|Joe Joe Group|41246|6|Mentioned|Map legend|Permian|Carboniferous|||||||
28230|Joe Joe Group|41270|6|Mentioned|p278|||||||||
28230|Joe Joe Group|41689|6|Mentioned|Table 1|||||||||
28230|Joe Joe Group|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
28230|Joe Joe Group|42491|6|Mentioned|p5|||Superseded Joe Joe Formation.||||||
28230|Joe Joe Group|42547|5|Briefly described|p80|||||||||
28230|Joe Joe Group|42614|5|Briefly described|p14|||Galilee Basin||||||
28230|Joe Joe Group|42641|6|Mentioned|Fig.3 P110|||||||||
28230|Joe Joe Group|42999|5|Briefly described|p94,Table1,p90|||||||||
28230|Joe Joe Group|46849|6|Mentioned|Fig. 7|||||||||
28230|Joe Joe Group|46881|6|Mentioned|Table 2|||||||||
28230|Joe Joe Group|47041|6|Mentioned|p164|||||||||
28230|Joe Joe Group|60295|5|Briefly described|p129|||Geological Province: Galilee Basin.||||||
28230|Joe Joe Group|60296|5|Briefly described|p156 Fig.1|Sakmarian||Geological Province: Galilee Basin||||||
28230|Joe Joe Group|61612|6|Mentioned|p270, p270 Fig. 1|Early Permian|Late Carboniferous|Geological Province: Bowen Basin. QLD.||||||17-MAR-09
28230|Joe Joe Group|63713|5|Briefly described|p1505, p1507 Fig.2, p1508, p1521, p1528|Sakmarian|Pennsylvanian|See also p1530, p1533. Fluvial to lacustrine sediments. According to the authors, includes Boonderoo Beds. Well-log correlation.|||Includes Jericho and Jochmus Formations, Lake Galilee Sandstone.|Is overlain by Aramac Coal Measures and Boonderoo Beds.||
28230|Joe Joe Group|63832|5|Briefly described|p131 fig 2, p134-135|Cisuralian|Serpukhovian|Of Galilee Basin. Spans the second (C2) to fifth (P1) glaciations.|||||Diamictites and rhythmically laminated mudrocks interbedded with fluvial conglomerates. The upper part has a thick succession of fluvial and lacustrine facies and some pyroclastic deposits with no evidence of glacial influence.|13-DEC-17
28230|Joe Joe Group|64288|5|Briefly described|p531-534, p543, p548, p552-553 |Sakmarian|Serpukhovian|Eastern Galilee Basin. Lower Namurian to Upper Asselian. Clearly shows that a cold-based ice sheet did not exist in this part of Godwana during the Pennsylvanian/Early Permian.|||Includes Lake Galilee Sandstone, Jericho Formation, Jochmus Formation and Aramac Coal Measures.|Is overlain by Reids Dome Beds.||
28230|Joe Joe Group|64631|5|Briefly described|p44 Fig.2, p48, 49.|Sakmarian|Mississippian|Galilee Basin. Contains intervals of proglacial strata. Some biostratigraphic age control. Age range seems to be different in N and Eastern margins. ?Time transgressive top from Asselian in N to Sakmarian in E. ||||Is overlain by Boonderoo Beds and Reids Dome Beds.||
28230|Joe Joe Group|64665|5|Briefly described|p53 Fig.2.|Early Permian|Early Permian|Galilee Basin.||||Is overlain by Aramac Coal Measures.||
28230|Joe Joe Group|65382|6|Mentioned|p715, p717 App. 2|Pennsylvanian|Pennsylvanian|Northeast Galilee Basin. The upper part of the group is constrained between 310 and 291 Ma.||||||
28230|Joe Joe Group|65489|5|Briefly described|p144 Fig.53|Permian|Late Carboniferous|Galilee Basin.||||Is overlain by Boonderoo Beds.||
28230|Joe Joe Group|66188|6|Mentioned|443, Fig 3|Early Permian|Late Carboniferous|Of the Galilee Basin. Includes Jochmus Formation, Jericho Formation, Oakleigh Sandstone.||||||
28230|Joe Joe Group|67323|5|Briefly described|p84|Permian|Carboniferous|Lovelle Depression, Galilee Basin.||||||
28230|Joe Joe Group|68279|6|Mentioned|p4, p7|Sakmarian|Bashkirian|Galilee Basin. Sedimentation in a freshwater fluvio-lacustrine system.|||Includes Jericho and Jochmus Formations.|||
28230|Joe Joe Group|68326|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Galilee Basin|||||Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|02-DEC-13
28230|Joe Joe Group|68328|5|Briefly described|Map legend.|Early Permian|Late Carboniferous||||||Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|68411|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Early Permian minimum age.||||Unconformably overlain by the Reids Dome beds. Unconformably underlain by the Ducabrook Formation.|Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|68414|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Galilee Basin.||||Overlain by Colinlea Sandstone (Back Creek Group). Underlain by the Ducabrook Formation.|Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|68423|5|Briefly described|map legend|Early Permian|Late Carboniferous|Galilee Basin.|||||Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Galilee Basin.||||||
28230|Joe Joe Group|68679|6|Mentioned|p375|Pennsylvanian|Pennsylvanian|Galilee Basin. Deposited during late Pennsylvanian-earliest Permian extension. See also Jo Jo Group (p469).||||||
28230|Joe Joe Group|68731|5|Briefly described|p198, pp200-201 Fig 3.110, p203|Early Permian|Mississippian|Continental, partly glaciogenic origin. Accorded Group status upon formal subdivision of the Joe Joe Formation. An unconformity, inferred from palynology, surface separates the Betts Creek beds from the Joe Joe Group.|||Includes Aramac Coal Measures, Jericho Formation, Lake Galilee Sandstone, and Jochmus Formation.|||14-JUL-14
28230|Joe Joe Group|68900|6|Mentioned|p4|Early Permian|Late Carboniferous|Drummond Basin.||||||
28230|Joe Joe Group|69379|5|Briefly described|map legend|Early Permian|Late Carboniferous||||||Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal|
28230|Joe Joe Group|70856|5|Briefly described|Map Legend|Permian|Late Carboniferous||||||Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|70857|5|Briefly described|Map Legend|Permian|Carboniferous|||||Overlain by Back Creek Group|Tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|71265|5|Briefly described|p589-590, p599-600, p603|Artinskian|Bashkirian|Galilee Basin. Sedimentary logs of CRD Montani 1 and OEC Glue Pot Creek 1.|||Jericho, Jochmus Formations; Aramac Coal Measures.|Is overlain unconformably by Rodney Creek Sandstone.||
28230|Joe Joe Group|71276|5|Briefly described|p286|Permian|Permian||||Aramac Coal Measures.|||
28230|Joe Joe Group|71701|4|Described|p153, p155-p156, p165, p167, p169|Cisuralian|Mississippian|Central Western Area, Galilee Basin. Thickest in the Koburra Trough where it reaches to 1781 m (Gray and Swarbrick, 1975). Lies in the APP1 and APP2 palynological zones.|||Includes the Aramac Coal Measures, Lake Galilee Sandstone, Jericho Formation and the Jochmus Formation.|Overlain by the Betts Creek Group.||
28230|Joe Joe Group|71710|4|Described|p370 Fig 3, p379, p385|Early Permian|Late Carboniferous|Geological province: southern Galilee Basin. Contains Namurian-Westphalian glacial diamictites in southern Galilee Basin. Parts reassigned to lower Jericho Formation (p376).|||Includes Jochmus Formation, Jericho Formation and Lake Galilee Sandstone.|Unconformably overlain by Colinlea Sandstone. Unconformably underlain by Ducabrook Formation of the southern Drummond Basin.||
28230|Joe Joe Group|72088|5|Briefly described|p8, p17, p28, p91|Cisuralian|Carboniferous|Lovelle Depression, Galileee Basin. Intersected in Galilee NS 2, NS 13 and Galilee NS 14/15R boreholes.|||Includes the Lake Galilee Sandstone, Jericho Formation, Aramac Coal Measures and the Jochmus Formation.||Glacigenic and fluvial sediments including tillitic conglomerate, lithic sandstone, siltstone, minor mudstone and coal.|
28230|Joe Joe Group|73117|6|Mentioned|p8|Permian|Carboniferous|Galilee Basin, southern. Palynological assemblages were described for the unit by Jones and Truswell (1992). Includes Verrucosisporites basiliscutus Oppel-zone (A), Brevitriletes leptoacaina Oppel-zone (B) and Diatomozonotriletes birkheadensis Oppel-zone (C) - all within the Spelaeotriletes queenslandensis Superzone.||||||
28230|Joe Joe Group|73163|5|Briefly described|p467-468, p470, p472, p476|Cisuralian|Cisuralian|Galilee Basin. Syndepositional and more ancient detrital zircons, some of Mesoproterozoic age, suggests that provenance of the Joe Joe Group is from the Thompson and New England orogens with the Anakie Province as a potential source of older zircons.|||Lake Galilee Sandstone, Jericho Formation, Jochmus Formation, Aramac Coal Measures, 'J and K' Seams.|Includes sandstone, siltstone, diamictite, tuff, minor conglomerate.|Predominantly composed of quartz with a minor feldspathic component. Lithic fragments of fine-grained volcanic and meta-sedimentary rocks.|
28230|Joe Joe Group|73472|6|Mentioned|p115|Sakmarian|Serpukhovian|Galilee Basin.|||Aramac Coal Measures, Jochmus Formation, Jericho Formation, Lake Galilee Sandstone|Equivalent to Boonderoo beds.||
30892|Joe-De-Little Granite|22675|4|Described|p94|Stephanian|Stephanian|Age: 301+/- 3Ma.||||||10-FEB-09
30892|Joe-De-Little Granite|23052|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30892|Joe-De-Little Granite|23161|4|Described|p41 table5|Early Permian|Late Carboniferous|Rb/Sr Age: 301 (+/-) 3 Ma.||||||
30892|Joe-De-Little Granite|43391|5|Briefly described|Map legend|Permian|Carboniferous|Carboniferous and/or Permian.||||||23-JUN-04
30892|Joe-De-Little Granite|44245|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30892|Joe-De-Little Granite|60659|5|Briefly described|p17, p81|Late carboniferous|Late Carboniferous|Includes diorite, hornblende-biotite granodiorite and hornblende-biotite granite. Intrudes Anakie Metamorphic Group and Ukalunda beds. Age: 301+/-3Ma.||||||07-FEB-11
30892|Joe-De-Little Granite|64851|5|Briefly described|Map legend|Permian|Carboniferous|Medium-grained hornblende-biotite granodiorite, diorite, pink hornblende-biotite granite.||||||
30892|Joe-De-Little Granite|70740|5|Briefly described|p34, 120, 126|Permian|Carboniferous|Outcrop characteristics briefly discussed. A whole rock Rb-Sr age of 301 +/- 3 Ma is given. Shown as Joe-de-Little Granodiorite p20, 28, 29.|Rb-Sr (bt and whole rock isochron) age of 301+/-3|||Intrudes the Les Jumelles beds, Ukalunda Formation and the Anakie Metamorphic Group. Faulted against the Sunbeam Granodiorite and the Ukalunda Formation.|Medium-grained, hornblende-biotite granodiorite, diorite, pink hornblende-biotite granite.|05-OCT-17
30892|Joe-De-Little Granite|73035|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Informal subdivision: Medium-grained hornblende-biotite quartz diorite to diorite.|||||Medium-grained hornblende-biotite granodiorite, diorite, pink hornblende-biotite granite.|
70428|John Clifford Road Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70428|John Clifford Road Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pale to dark pink, medium-grained, uneven-grained, leucocratic alkali feldspar granite.|
70428|John Clifford Road Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pale to dark pink, medium-grained, uneven-grained, leucocratic alkali feldspar granite.|
70428|John Clifford Road Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, medium-grained, seriate, leucocratic alkali feldspar granite; sodic amphibole, microperthite. A-type, alkaline.|
70428|John Clifford Road Granite|73450|4|Described|p15-19, p21, p35|late Triassic|late Triassic|[Also written as John Clifford Granite, p17]. Previously included in the Miriam Vale Granodiorite (Ellis, 1974); delineated as a discrete unit during subsequent mapping by GSQ. Forms a small, irregular, NE-aligned pluton or plutons centred on Lowmead. Very poorly exposed and forms low, undulating country. Unconformably overlain by relict flows of Tertiary basalt.||||Intrudes Glenelm Granite, Hawthorne Granite, Diamond Head Granite and Rosevale Granite.|Pale to dark pink, medium-grained, uneven grained alkali feldspar granite.|
35194|Johnstone Creek Igneous Complex|23042|5|Briefly described|p97,8 Fig 2|Permian|Carboniferous|||||||
35194|Johnstone Creek Igneous Complex|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35194|Johnstone Creek Igneous Complex|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Dark grey, medium-grained, equigranular hornblende diorite to granodiorite; medium to coarse-gr. sub-equigranular biotite granite; local pegmatite and aplite; intruded by andesite, microdiorite and rhyolite dykes.||||||
35194|Johnstone Creek Igneous Complex|65388|3|Fully described|p371-372,135 Fig. 53, 362, 364, 365, 380|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Relationships unknown, but dyke swarms suggest age is Early Permian or older. Light greenish grey coarse-grained equigranular biotite-hornblende granodiorite in type section. Also misspelt as Johnston Creek Igneous Complex p371. Said to separate two outcrops of Gargett Granite. Also misspelt as Mount Johnstone Igneous Complex p380.||||||
35194|Johnstone Creek Igneous Complex|68679|6|Mentioned|p366 Fig.5.57|||REE plot.||||||
32135|Jonah Vale Granite|23037|4|Described|p82,3|Permian|Silesian|||||||
32135|Jonah Vale Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgjv].  Pale pink to white, medium- to coarse-grained biotite granite.||||||
32135|Jonah Vale Granite|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32135|Jonah Vale Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pale pink to white, medium- to coarse-grained, biotite granite.||||||
32135|Jonah Vale Granite|60282|6|Mentioned|p19, p21|||See also p22.||||||
32135|Jonah Vale Granite|65388|4|Described|p260, p236, 237, 238, 248, 259, 272|Early Permian|Late Carboniferous|Interpreted as older than Dawson Granite. Relationship to adjacent Pinedale Granite and Glandore Granodiorite is unknown due to poor outcrop. Radiometric response compared with Hildura Quartz Monzodiorite. Mainly pink to white, medium to coarse-grained, hornblende-biotite granite. ||||||
32135|Jonah Vale Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Relationships with surrounding units unknown. Intruded by grey porphyritic granite dykes near eastern edge.|||||Pink to grey, medium-grained hornblende-biotite granite.|
78572|Jones Dam Suite|68731|5|Briefly described|p148, p149|Middle Ordovician|Middle Ordovician|Rienks, Tenison, Woods and Wyborn (1979). Contains trondhjemites with some A-type affinities. Chemically distinctive and of limited extent. No geochronology is available, but strained quartz grains and recrystallised biotite suggest an Ordovician age.||Of the Carse Creek Complex.|||Comprises grey, medium-grained, subequigranular, biotite-hornblende granodiorite in places grading into a monzogranite.|19-DEC-13
34665|Jones Dam Supersuite|22847|6|Mentioned|p 10|||||||||
34665|Jones Dam Supersuite|23422|4|Described|p173, p209 Table 6.6|||Probably Ordovician.||||||
34665|Jones Dam Supersuite|23893|5|Briefly described|p12|Middle Ordovician|Late Cambrian|Geological Province: Macrossan Province.||||||
34665|Jones Dam Supersuite|68731|6|Mentioned|p148, p149|||||||||
24322|Juandah Coal Measures|12597|5|Briefly described|p496, p505-506|||Mimosa Syncline area, Clarence-Moreton Basin. 50-200m thick. Very similar lithologies to Taroom Coal Measures. Coal deposits and properties described in some detail.||Unit in Walloon Coal Measures.|||Lithic and feldspathic sandstone, siltstone, mudstone and coal.|
24322|Juandah Coal Measures|37990|6|Mentioned|p185|||||||||
24322|Juandah Coal Measures|37993|3|Fully described|p162|||||||||
24322|Juandah Coal Measures|38658|6|Mentioned|p153|||||||||
24322|Juandah Coal Measures|40675|6|Mentioned|Table 9A|||||||||
24322|Juandah Coal Measures|63218|4|Described|pp209-221.     |Middle Jurassic|Middle Jurassic|Surat Basin. Contains seven named seams. The article details analyses for coal seam gas.||Unit in Walloon Subgroup.||Overlies Tangalooma Sandstone.||16-NOV-12
24322|Juandah Coal Measures|64665|5|Briefly described|p61.|Middle Jurassic|Middle Jurassic|||Unit in Walloon Subgroup.|Includes Juandah Sandstone.|||
24322|Juandah Coal Measures|64856|5|Briefly described|p87|Middle Jurassic|Middle Jurassic|Of the Walloon Coal Measures (Subgroup) of Jones and Patrick (1979). Middle Jurassic age implied.| | ||||31-JAN-13
24322|Juandah Coal Measures|65003|5|Briefly described|p1-2, p20, p26, p27-29, 31-32|Middle Jurassic|Early Jurassic|.||Of Walloon Subgroup, Surat Basin.||Overlain by the Kumbarilla beds.|Incorporates high volatile perhydrous, and bituminous rank coal, with high ash content.|30-MAR-12
24322|Juandah Coal Measures|65096|5|Briefly described|p372, p368, p370 Fig.2, |Middle Jurassic|Middle Jurassic|Of Jones and Patrick (1981). Up to 300m thick. Said to be subdivided into, in ascending order, the Argyle, Iona, Wambo, MacAlister, and Kogan seam packages.||Of the Walloon Coal Measures/Walloon Subgroup.||||
24322|Juandah Coal Measures|67133|6|Mentioned|p12-13|||Presented as Lower and Upper Juandah Coal Measures citing the "latest proposed stratigraphy" (Hamilton, 2007).||Walloon Subgroup.||||
24322|Juandah Coal Measures|67402|6|Mentioned|p275|||Surat Basin.||Walloon Subgroup||Overlies the Taroom Coal Measures.||
24322|Juandah Coal Measures|68117|4|Described|p345-355|Middle Jurassic|Middle Jurassic|Jones and Patrick (1981) after Swarbrick (1973)'s intervals 7 and 8 of Injune Creek Group. 70-270m thick. Informally divided into lower and upper units, separated between Nangram and Lower Macalister Seams, based on coal petrology. Coal analysis; coal seam gas characteristics.||Walloon Subgroup.|Argyle, Iona, Wambo, Nangram, Macalister (Lower and Upper), Kogan Seams.|Conformably overlies Tangalooma Sandstone. Is overlain unconformably by Springbok Sandstone.|Grey to black, carbonaceous in part, laminated mudstone with well-preserved plant fossils; grey, partly micaceous siltstone; light-grey, fine- to medium-grained, moderately sorted and lithic labile sandstone; and coal.|
24322|Juandah Coal Measures|68139|5|Briefly described|p21, p25 Fig.4, p27, 29-31, 33|Middle Jurassic|Middle Jurassic|Surat Basin. Maceral composition tabulated, discussed.||Walloon Subgroup.|Lower, Upper, Juandah Coal Measures.|Overlies Tangalooma Sandstone. Is overlain by Springbok Sandstone.||
24322|Juandah Coal Measures|69574|6|Mentioned|p21, 23-24, 26, 28, 31-32|Middle Jurassic|Middle Jurassic|Surat Basin. Desorbed gas molecular composition and compound-specific isotopes tabulated.||Walloon Subgroup.|Juandah Coal Measures, Lower and Upper; Juandah Sandstone.|||
24322|Juandah Coal Measures|69594|6|Mentioned|p536|||Jones and Patrick (1981) raised the Walloon Coal  Measures to Subgroup status and included this unit, as well as the Tangalooma Sandstone and Taroom Coal Measures. In this study, they are regarded as Members of the Walloon Coal Measures only in the NE Surat Basin.||||||
24322|Juandah Coal Measures|69790|5|Briefly described|p1061, p1065-1078|||Jones and Patrick (1981). Contains three informal members: lower and upper Juandah Coal Measures and Juandah sandstone. Inferred depositional environment was lower fluvial, immediately upstream of a delta.||Unit in Walloon Subgroup.|Three informal units [?Members]: lower and upper Juandah Coal Measures and Juandah sandstone.|Overlies Tangalooma Sandstone and Taroom Coal Measures. Is overlain unconformably by Springbok Sandstone.||
24322|Juandah Coal Measures|70374|5|Briefly described|p809 figure 1, p810,811|Oxfordian|Oxfordian|CA-TIMS date from tuff towards the base of the unit in Stratheden 4, eastern Surat Basin.|158.86 +/- 0.04 Ma (Zircons)|Walloon Coal Measures /Walloon Subgroup.|Shown as including[invalid unit name] Juandah Sandstone.|||
24322|Juandah Coal Measures|70628|5|Briefly described|p952-953,957,964-965|Callovian|Bathonian|Upper coal layer. Mostly discussed as the subdivided  upper and lower Juandah Coal Measures.||Walloon Subgroup|Said to include [invalid] Juandah Sandstone (also called Wambo Sandstone) dividing Upper and Lower Juandah Coal Measures.|Underlies Springbok Formation. Overlies Tangalooma Sandstone|Sand, coal, maceral trends indicate drying upward trend during deposition.|30-JUN-16
24322|Juandah Coal Measures|71282|5|Briefly described|p456, p457 Fig.1|||Jones and Patrick (1981). Surat Basin. [The authors of this article incorrectly state that Jones and Patrick "informally" named this unit.]||Walloon Subgroup.||Overlies Tangalooma Sandstone.||
24322|Juandah Coal Measures|72297|5|Briefly described|p699, p751|Jurassic|Jurassic|NE Surat Basin. Production started in 1994 at the Wilkie Creek open-cut mine. Elsewhere this is part of the Walloon Coal Measures.||Walloon Subgroup.|Argyle, Iona, Wambo, Nangram, Macalister Lower, Macalister Upper, Kogan Seams.|Overlies Tangalooma Sandstone. Is overlain by Springbok Sandstone.||
79046|Juandah Coal Measures, lower|69790|5|Briefly described|p1061, p1066-1073, p1078|||Informal name for a division within Juandah Coal Measures. Gamma-ray logs and isopach maps, coal plies and thickness, and lithofacies percentages are all detailed. Mined at Onaview, Wilkie Creek and Kogan Creek.||Unit in Juandah Coal Measures.||Is overlain by Juandah sandstone or unconformably by Springbok Sandstone.||
79046|Juandah Coal Measures, lower|70374|6|Mentioned|p809 figure 1,|Oxfordian|Oxfordian|||Juandah Coal Measures||||
79047|Juandah Coal Measures, upper|69790|5|Briefly described|p1061,p1066-1067,p1070-1073,p1078 Fig.17|||Informal name for a division within Juandah Coal Measures. Gamma-ray logs and isopach maps, coal plies and thickness, and lithofacies percentages are all detailed. Represents a floodplain-mire sequence containing up to three major coal intervals which are completely absent in the southern part of the study area. Mined at Wandoan. Has more thick (>5m) coals than any other unit in Walloon Subgroup.||Unit in Juandah Coal Measures.||Overlies Juandah sandstone.||
79047|Juandah Coal Measures, upper|70374|6|Mentioned|p809 figure 1,|Oxfordian|Oxfordian|||Juandah Coal Measures||||
33135|Judas Trachybasalt|24489|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.||||||
33135|Judas Trachybasalt|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kggj].  Grey porphyritic biotite-hornblende augite trachybasalt cut by porphyritic syenite dykes.||||||
33135|Judas Trachybasalt|68008|3|Fully described|p444-445, p447, p454-458|Early Cretaceous|Early Cretaceous|Defined in this study; previously mapped but not named by Neale (1968). Covers c.1 km2 N from Tollbar Creek to the summit of Judas Mountain (from which its name is derived). The type area is along Tollbar Creek. Geophysics briefly described. Geochemistry detailed: compared with Ridler Monzonite.||Glassford Igneous Complex.||Intrudes Ridler Monzonite.|Grey, porphyritic trachybasalt; phenocrysts include plagioclase, augite and hornblende to 1cm across. K-feldspar-phyric dykes cut the trachybasalt.|
33135|Judas Trachybasalt|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Burns Spur Nepheline Monzosyenite, Goondicum Gabbro, Radley Nepheline Syenite, Ridler Monzonite, Tollbar Breccia, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
33135|Judas Trachybasalt|69594|5|Briefly described|p560-561|Cretaceous|Cretaceous|Whitsunday Volcanic Province.||Glassford Igneous Complex.||Relationships with other units unknown.|Grey, porphyritic, biotite-hornblende-augite trachybasalt with euhedral phenocrysts of plagioclase, augite and hornblende; cut by porphyritic syenite dykes.|
33135|Judas Trachybasalt|73450|4|Described|p11, p60-64, p66|early Cretaceous|early Cretaceous|Delineated by Neale (1968); briefly examined and defined by Murray et al. (2012). Forms steep, hilly to mountainous country north of Tollbar Creek; supports a fairly dense tree and grass cover. Surrounded by the Ridler Monzonite; interpreted to be related to it, thus was deemed coeval (Murray et al., 2012). May be related to the Radley Nepheline Syenite, Ridler Monzonite, and Burns Spur Nepheline Monzosyenite.||Glassford Igneous Complex|||Grey, porphyritic trachybasalt with up ca 30-40 percent phenocrysts of mainly calcic plagioclase, augite and hornblende up to 1 cm across.|
25723|Judea Formation|23032|4|Described|p20,52|Early Silurian|Early Ordovician|||||||
25723|Judea Formation|23290|6|Mentioned|p6|||||||||
25723|Judea Formation|23291|6|Mentioned|p27|||Geological Province: Georgetown Region.||||||08-JUL-15
25723|Judea Formation|23423|5|Briefly described|p267||Early Ordovician|Broken River Province||||||
25723|Judea Formation|23424|5|Briefly described|Table 8.1 Fig 8.3 p332.||Early Ordovician|Age: Tetragraptid in sedimentary upper part of Judea Formation indicates an early Ordovician age. Graveyard Creek Subprovince. Maximum thickness <1500 m.||||||
25723|Judea Formation|23430|4|Described|p476-477|||Underlying Unit Graveyard Creek Group. Broken River Province.||||||
25723|Judea Formation|23431|5|Briefly described|p541|||||||||
25723|Judea Formation|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Volcanic No. V43.||||||
25723|Judea Formation|23616|5|Briefly described|Table 1C p15|||May be equivalent to Mulgrave Formation. Broken River Province.||||||
25723|Judea Formation|23619|4|Described|p34 Table 1||Early Ordovician|Faulted against Halls Reward Metamorphics and Wairuna Formation. Also see p7. Graveyard Creek Subprovince of the Broken River Province.||||||
25723|Judea Formation|23713|5|Briefly described|p13|Early Silurian|Early Ordovician|||||||
25723|Judea Formation|23893|5|Briefly described|p9 Fig. 4|Early Devonian|Ordovician|||||||
25723|Judea Formation|24029|5|Briefly described|p111, p113 Fig.2|Ordovician|Ordovician|Tectonized turbidites.||||||
25723|Judea Formation|24485|5|Briefly described|p27|Early Ordovician|Early Ordovician|||||||
25723|Judea Formation|24577|4|Described|p752 Fig. 1|Ordovician|Ordovician|Overlain by the Wairuna Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
25723|Judea Formation|24613|5|Briefly described|p6 Fig. 3|Early Devonian|Ordovician|Geological province: Burdekin Basin.||||||07-FEB-11
25723|Judea Formation|40787|5|Briefly described|p322|||||||||
25723|Judea Formation|41260|3|Fully described|p29|||Described p105.||||||06-MAY-15
25723|Judea Formation|41675|6|Mentioned|p14|||||||||
25723|Judea Formation|41679|6|Mentioned|p255|||||||||
25723|Judea Formation|41719|1|Redefined|p215|Middle Ordovician||Originally Judea Beds.||||||10-APR-08
25723|Judea Formation|41739|6|Mentioned|Fig.1|||See also Fig.2||||||
25723|Judea Formation|42031|5|Briefly described|Fig.4 P761|||||||||
25723|Judea Formation|42054|6|Mentioned|p273|||||||||
25723|Judea Formation|42279|6|Mentioned|p26|||||||||
25723|Judea Formation|42407|6|Mentioned|p36|||||||||
25723|Judea Formation|42692|5|Briefly described|map legend|Ordovician||||||||
25723|Judea Formation|42693|5|Briefly described|map legend|Ordovician||||||||
25723|Judea Formation|42709|6|Mentioned|map legend|||||||||
25723|Judea Formation|42752|5|Briefly described|p47|||||||||
25723|Judea Formation|42933|1|Redefined|p48|Early Silurian|Early Ordovician|||||||
25723|Judea Formation|43060|5|Briefly described|p39|||||||||
25723|Judea Formation|43083|5|Briefly described|??location?|||||||||17-JUN-09
25723|Judea Formation|43113|4|Described|Table 1 p21||Early Ordovician|||||||
25723|Judea Formation|43213|6|Mentioned|p66|Ordovician|Ordovician|Quartzose flysch sediments, preserved as thrust slices.||||||
25723|Judea Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
25723|Judea Formation|43259|4|Described|Appendix 1,p4.||Ordovician|||||||
25723|Judea Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
25723|Judea Formation|43480|6|Mentioned|26|||||||||
25723|Judea Formation|43625|6|Mentioned|p20|||Age: Early-Middle Ordovician (probably)||||||
25723|Judea Formation|43664|6|Mentioned|p83||Ordovician|||||||
25723|Judea Formation|43772|6|Mentioned|p786|||||||||
25723|Judea Formation|50093|6|Mentioned|p329|||Onlapped by Storm Hill Sandstone.||||||07-FEB-11
25723|Judea Formation|50202|5|Briefly described|Map legend|Ordovician|Ordovician|Fine-grained quartzose arenite and mudstone.||||||
25723|Judea Formation|60425|6|Mentioned|p20|Early Ordovician|Early Ordovician|In the Broken River Province. Correlates with Mulgrave Formation.||||||07-FEB-11
25723|Judea Formation|61211|5|Briefly described|p274|Early Ordovician|Early Ordovician|Overlie rocks of the Gray Creek Complex. ||||||
25723|Judea Formation|63152|5|Briefly described|p120 Fig. 3|Early Ordovician|Early Ordovician|Includes Donaldsons Well Member. Turbiditic quartzose arenites and mudstones with volcaniclastic arenites locally.||||||
25723|Judea Formation|63154|5|Briefly described|p281 Fig. 3|Early Ordovician|Ordovician|Includes Donaldson Well volcanic member (informal). Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
25723|Judea Formation|67455|6|Mentioned|p576 Fig.2, p587.|Early Ordovician|Early Ordovician|Low-grade metamorphism.||||Overlies Gray Creek Complex.||
25723|Judea Formation|67848|5|Briefly described|p1, p3, Fig.2, p4, p5 Fig.3, pp12-15.|Early Ordovician|Early Ordovician|Continent-derived, deep marine sedimentary and volcanic strata; cover for oceanic crust (Gray Creek Complex). Age from a Bendigonian graptolite.||||Overlies Gray Creek Complex. Is intruded by Netherwood Tonalite.|Quartz-rich turbidites and bimodal volcanics.|
25723|Judea Formation|68336|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||Includes Donaldsons Well Volcanic Member.||Fine-grained quartzose sandstone and mudstone; local melange.|
25723|Judea Formation|68341|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||Includes Donaldsons Well Volcanic Member.||Fine-grained quartzose sandstone and mudstone; local melange.|
25723|Judea Formation|68344|5|Briefly described|Map legend.|Ordovician|Ordovician|Graveyard Creek Subprovince, Broken River Province.|||||Fine-grained quartzose arenite and mudstone; local melange.|
25723|Judea Formation|68478|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince. The 2 facies are mapped separately. Contains evidence of a Late Ordovician (?) deformation event which produced bedding parallel cleavage.|||Includes Donaldsons Well Volcanic Member.||Fine-grained quartzose sandstone and mudstone; local melange.|
25723|Judea Formation|68479|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince. The 2 facies are mapped separately. Contains evidence of a Late Ordovician (?) deformation event which produced bedding parallel cleavage.|||Includes Donaldsons Well Volcanic Member.||Fine-grained quartzose sandstone and mudstone; local melange.|
25723|Judea Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Broken River Province. ||||||
25723|Judea Formation|68576|5|Briefly described|Q_11: p34-36, p39|Early Ordovician|Early Ordovician|Greenvale area. Part of the Thomson Orogen. Basement to the Silurian-Devonian Graveyard Creek Subprovince (Broken River Province). Strongly deformed: tight to isoclinally folded, strong cleavage, locally boudinaged.||||Is faulted against Gray Creek Complex.|Quartzose sandstone and strongly-cleaved mudstone.|
25723|Judea Formation|68731|6|Mentioned|p221|||||||||
25723|Judea Formation|69030|5|Briefly described|p6|Ordovician|Ordovician|Graveyard Creek Subprovince (Broken River Province).|||Donaldson Well Volcanic Member.|Is intruded by Netherwood and Saddington Tonalites.||
25723|Judea Formation|69592|4|Described|p231, p251 Fig.4.35, p252-255, p258-259|Early Ordovician|Early Ordovician|See also p261 Fig.4.50, p266-268, p270, p297. Graveyard Creek Subprovince, Broken River Province. Part of the basement assemblage. Similar lithologies to Mulgrave Formation. The upper sedimentary interval is >500m thick. Consistent with a backarc volcanic assemblage. Folded and metamorphosed by the Benambran Orogeny to greenschist grade; melange zones occur near Greenvale and Halls Reward Fault.|||Donaldsons Well Volcanic Member.|Is overlain unconformably by Crooked Creek Conglomerate and Poley Cow Formation (Graveyard Creek Group), or Storm Hill Sandstone. Is intruded by Netherwood Tonalite. Abuts the Gray Creek Complex.|Deep-marine, fine- to very fine-grained or silty quartz sandstones (turbidites), pelite beds with variably developed slaty cleavage; overlying mafic/bimodal volcanic rocks (Donaldsons Well Volcanic Member).|
25723|Judea Formation|70207|6|Mentioned|p94|Ordovician|Ordovician|Mentioned as having similarities with, and thus probably coeval with, Mulgrave Formation. The latter turns out to be significantly younger.||||||
25723|Judea Formation|70744|5|Briefly described|p947|Ordovician|Ordovician|Graveyard Creek Subprovince, Mossman Orogen. Marks the accretion of a Late Ordovician island arc to the continental margin during the Benambran Orogeny.|||||Quartz-rich turbidites.|
25723|Judea Formation|71031|5|Briefly described|p4-p5, p71|Lower Ordovician|Lower Ordovician|Thomson Orogen, Broken River Province. ||||||
25723|Judea Formation|73201|6|Mentioned|p610-611, p613|Ordovician|Cambrian|Broken River Province. Graveyard Creek Subprovince. Contains an Ordovician graptolite.  Age given as late Cambrian to Ordovician.||||||
41622|Jug Microgranite|60357|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Kennedy Province. Porphyritic granite, minor vitrophyre.||||||
23675|Julago Volcanics|23422|4|Described|p184, p204 Table 6.3|Early Permian|Early Permian|Defined by Trezise et al. (1989). Maximum thickness: 500m. Age from flora and intruding granites.||||||25-MAY-04
23675|Julago Volcanics|23430|5|Briefly described|p504 Table 14.5|||Also see p518.||||||
23675|Julago Volcanics|23431|5|Briefly described|p538|||||||||
23675|Julago Volcanics|23509|5|Briefly described|Map Legend||Permian|||||||
23675|Julago Volcanics|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V54. Assumed to be I-Type.||||||
23675|Julago Volcanics|23893|4|Described|p21|Early Permian|Early Permian|Geological Province: Kennedy Province.||||||
23675|Julago Volcanics|40607|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
23675|Julago Volcanics|40954|6|Mentioned|p133|||||||||
23675|Julago Volcanics|43259|4|Described|Appendix 1,p5.||Permian|||||||
23675|Julago Volcanics|43935|5|Briefly described|Map Legend||Permian|||||||
23675|Julago Volcanics|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Charters Towers Province.||||||
23675|Julago Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek, Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Little Fork, Mitchell River and Nychum Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
23675|Julago Volcanics|68576|5|Briefly described|Q_11: p44|Permian|Permian|Townsville. Part of the Kennedy Igneous Association. Sedimentary interbeds contain Glossopteris flora.|||||Felsic to intermediate volcanics with interbedded sedimentary intervals. Intruded by granite and a swarm of mafic and felsic dykes.|
23675|Julago Volcanics|68731|5|Briefly described|p204||Middle Permian|Tresize, Holmes and Cooper (1989). Described but not named by Wyatt et al. (1970), Stephenson (1970) and Stephenson and Patrick (1978). Outcrops near Townsville. ~ 300-500 m thick. Basal part contains mid-Permian macroflora including Glossopteris.|||||Comprises a basal succession of volcaniclastic conglomerate, sandstone, siltstone, and mudstone, locally containing thin seams. This is followed by andesitic to rhyolitic lavas.|
23675|Julago Volcanics|69593|5|Briefly described|p495, p497|Permian|Permian|Townsville region. Intermediate to felsic volcanics with intercalated sediments. Early-mid Permian fossils (including Glossopteris) suggest possible link with Bowen Basin.||||Equivalent to Lizzie Creek Volcanic Group.|Basal sedimentary assemblage, including coal, overlain by andesitic to rhyolitic lavas and volcaniclastic rocks. I-type.|
22043|Jumna Granite|23423|6|Mentioned|p304 table 7.3|||||||||
22043|Jumna Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: ~314Ma Rb-Sr.||||||
22043|Jumna Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 250. I-Type.||||||
22043|Jumna Granite|23616|6|Mentioned|Table 1C p44|||||||||
22043|Jumna Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supoersuite). Pink to cream, coarse to medium biotite granite; aplite. Age: 313Ma.||||||15-JUN-06
22043|Jumna Granite|43259|4|Described|Appendix 1,p33.||Late Carboniferous|Age is 313 Ma.||||||
22043|Jumna Granite|60425|4|Described|p45 Tb. 3, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Sup'suite). Age:~314Ma (Rb-Sr). Unconform.below/or intruded by Slaughter Yard Creek Volcs. Coarse- to medium-grained biotite granite, subordinate aplitic microgranite; cassiterite-bearing greisen zones common; I-type.||||||07-FEB-11
22049|Junevale Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Junevale Suite (Ootann Supersuite). Intruded by Gelaro, Rices Creek Granites. Ages: ~300 and 313 Ma. Geological Province: Georgetown Region.||||||08-JUL-15
22049|Junevale Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
22049|Junevale Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 376. I-Type.||||||
22049|Junevale Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22049|Junevale Granite|23624|4|Described|p12|Permian|Carboniferous|Parent: Ootann Supersuite.||||||17-DEC-13
22049|Junevale Granite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
22049|Junevale Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
22049|Junevale Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, porphyritic hornblende-biotite and biotite monzogranite, with numerous enclaves; subordinate fine-grained, porphyritic biotite monzogranite.|
22049|Junevale Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, porphyritic hornblende-biotite and biotite monzogranite, with numerous enclaves; subordinate fine-grained, porphyritic biotite monzogranite.|
22049|Junevale Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Pink, fine to medium-grained, porphyritic hornblende-biotite and biotite granite.|
37886|Junevale Suite|23291|5|Briefly described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
26309|Juntala Metamorphics|22963|5|Briefly described|p69||Paleoproterozoic|Correlates to the Mt Isa Glen Idol Schist and lower sequence of the Willyama Supergroup.||||||07-NOV-08
26309|Juntala Metamorphics|23032|4|Described|p9,49,50|Paleoproterozoic|Paleoproterozoic|Grade into Einasleigh Metamorphics. Deformed 1550Ma to 1560Ma. Primary age late Palaeoproterozoic (~ 1700-1650Ma).||||||07-NOV-08
26309|Juntala Metamorphics|23220|5|Briefly described|Fig.2 p9|||Correlate of Einasleigh metamorphics and Corbett Formation. Of Etheridge Group.||||||16-JAN-07
26309|Juntala Metamorphics|23291|4|Described|p87 Tb. 3.6p|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Geological Province: Georgetown Region.||||||08-JUL-15
26309|Juntala Metamorphics|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26309|Juntala Metamorphics|35920|6|Mentioned|p26|||||||||
26309|Juntala Metamorphics|35921|5|Briefly described|p31|||To be defined by A.Duncan.||||||
26309|Juntala Metamorphics|36937|6|Mentioned|p229|||||||||
26309|Juntala Metamorphics|37576|6|Mentioned|p8|||||||||
26309|Juntala Metamorphics|37609|6|Mentioned|p307|||See also p309.||||||16-JAN-07
26309|Juntala Metamorphics|38714|6|Mentioned|p182|||||||||
26309|Juntala Metamorphics|38715|2|Defined|p191|Mesoproterozoic|Mesoproterozoic|Formerly "Juntala Schist".||||||16-JAN-07
26309|Juntala Metamorphics|39445|5|Briefly described|Table 2|||See also p45||||||16-JAN-07
26309|Juntala Metamorphics|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
26309|Juntala Metamorphics|39924|6|Mentioned|Fig.2|||||||||
26309|Juntala Metamorphics|41975|6|Mentioned|p432|||||||||
26309|Juntala Metamorphics|42199|5|Briefly described|Table 1 P280|||||||||
26309|Juntala Metamorphics|43286|5|Briefly described|Map Legend||Proterozoic|Of Etheridge Group.||||||16-JAN-07
26309|Juntala Metamorphics|43603|5|Briefly described|p6||Proterozoic|||||||
26309|Juntala Metamorphics|43664|4|Described|p20-21|||||||||
26309|Juntala Metamorphics|50200|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26309|Juntala Metamorphics|50211|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Etheridge Group.||||||07-NOV-08
26309|Juntala Metamorphics|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||19-AUG-04
26309|Juntala Metamorphics|61258|5|Briefly described|p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Georgetown Inlier. See also p388 Fig. 2. ||||||07-NOV-08
26309|Juntala Metamorphics|64707|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Comprises mica schist and quartzite westwards into gneiss; mica schist, locally carbonaceous; amphibolite.||||||
26309|Juntala Metamorphics|65887|5|Briefly described|p40 Fig.1, p41 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||
26309|Juntala Metamorphics|66800|6|Mentioned|p926 Table 1.|||||||Overlies Einasleigh Metamorphics.||
26309|Juntala Metamorphics|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||Overlies Einasleigh Metamorphics.||
26309|Juntala Metamorphics|67430|6|Mentioned|p25|||||||||
26309|Juntala Metamorphics|68338|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|||||Amphibolite; mica schist, locally carbonaceous; mica schist and quartzite grading westwards into gneiss.|
26309|Juntala Metamorphics|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. The three facies are mapped separately.||Unit in Etheridge Group.|||Mica schist and quartzite grading into gneiss; mica schist, locally carbonaceous; amphibolite.|
26309|Juntala Metamorphics|68410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Shown as older than D1 (> 1560 Ma, < 1590 Ma?) and younger than 1670 Ma. Contains 4 unnamed subunits.|1670 - 1560 Ma||||Amphibolite; carbonaceous mica schist; mica schist, locally carbonaceous; mica schist and quartzite grading westwards into gneiss.|
26309|Juntala Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. This unit, as well as the Robertson River Subgroup, Cassidy Creek and McDevitt Metamorphics, are all mapped under the symbol, -Per.||Unit in Etheridge Group.||||
26309|Juntala Metamorphics|69591|5|Briefly described|p61-63, p65|Paleoproterozoic|Paleoproterozoic|Werrington area, southern Georgetown Inlier. Underwent lower amphibolite-grade metamorphism, but extensive retrogression is evident. Grades W and N into the Einasleigh Metamorphics. Closely resembles the schist facies of Corbett Formation.||Etheridge Group.||Is faulted against Einasleigh Metamorphics. Is intruded by Cobbold Metadolerite.|Predominantly mica schist, with a locally persistent graphitic mica schist horizon; minor quartzite.|
39538|Kabra Quartz Monzodiorite|23799|5|Briefly described|p117|||Of Littlemore Suite.  Geological Province: Yarrol Province.||||||
39538|Kabra Quartz Monzodiorite|24615|5|Briefly described|CD|Triassic|Triassic|[Rgbk].  Altered grey medium-grained hornblende quartz monzodiorite, dark grey hornblende-augite quartz gabbro, hornblende-hypersthene-augite-biotite gabbro.||||||
39538|Kabra Quartz Monzodiorite|50209|5|Briefly described|Map Legend|Triassic|Triassic|Of the Bouldercombe Igneous Complex.||||||17-MAY-04
39538|Kabra Quartz Monzodiorite|50317|5|Briefly described|Map Legend|Triassic|Triassic|Of the Bouldercombe Igneous Complex.||||||
39538|Kabra Quartz Monzodiorite|68008|2|Defined|p334, p337, p357, p361, p363-366, p621|Triassic|Permian|Clearly defined by aeromagnetics. Forms an elongate mass 10 x 4 km, centred 15km SW of Rockhampton. Named after the township and railway siding of Kabra. The type area is Table Mountain; good exposures as boulders and in cuttings along the road to the summit tower. Geophysics briefly described and modelled; geochemistry described. Associated with two small magnetite-rich skarns in and at the contact with Rockhampton Group. No age determination; relative age from relationships with other units.||Bouldercombe Igneous Complex.||Intrudes Gracemere Gabbro; Raspberry Creek, Mount Alma, Lorray Formations; Rockhampton Group and ?Bundaleer Tonalite.|Hornblende quartz monzodiorite. Subhedral zoned laths of calcic andesine comprise 65-70% of the rock. More mafic in the south and central parts where it is quartz gabbro.|
39538|Kabra Quartz Monzodiorite|68679|5|Briefly described|p424-427|||Yarrol Province. An elongate, ~10 x 4km unit along the northern margin of the eastern lobe of the Complex. Geochemistry briefly described.||||Intrudes Raspberry Creek, Mount Alma, Lorray Formations and the Rockhampton Group; and possibly the Bundaleer Tonalite, Gracemere Gabbro and the (undivided) Bouldercombe Igneous Complex.|Altered hornblende-quartz monzodiorite, hornblende-augite-quartz gabbro, hornblende-hypersthene-augite-biotite-quartz gabbro.|
39538|Kabra Quartz Monzodiorite|73450|6|Mentioned|p52|Triassic|Triassic|||||||
30699|Kahko Granodiorite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30699|Kahko Granodiorite|50536|5|Briefly described|p1.5, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30699|Kahko Granodiorite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event.||Sybella Suite|||Foliated to gneissic, medium- to coarse-grained biotite-hornblende granodiorite and minor diorite; extensively intruded by porphyritic biotite granite, leucogranite and tourmaline-bearing pegmatite.|
30699|Kahko Granodiorite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Foliated to gneissic medium- to coarse-grained biotite-hornblende granodiorite and minor diorite; intruded by porphyritic biotite granite, leucogranite and pegmatite.|
70657|Kalee Park Intrusive Complex|23251|6|Mentioned|p40|||See also Kallee Park Intrusive Complex - unclear which spelling is correct?||||||
41317|Kalkadoon Suite|50536|5|Briefly described|p1.4, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1860Ma.||||||07-NOV-08
41317|Kalkadoon Suite|63866|5|Briefly described|p54, p56-p57|Orosirian|Orosirian|Southern McArthur Basin.|c. 1860-1845 Ma|||Equivalent to the Scrutton Volcanics.||
41317|Kalkadoon Suite|65396|6|Mentioned|p301|||See Kalkadoon Granite. Considered by Budd et al. (2002) to have little or no metallogenic potential in the Mount Isa Inlier.||||||
41317|Kalkadoon Suite|66882|5|Briefly described|p117|Orosirian|Orosirian|Discussed but rejected as possible source for felsic juvenile material in Cleve Group.|c.1860 Ma||Includes Leichhardt Volcanics.|||03-MAR-15
41317|Kalkadoon Suite|67323|5|Briefly described|p14, p40-41|||Kalkadoon-Leichhardt Domain, central Mount Isa Block. Variation on Kalkadoon Supersuite.|||Said to include Kalkadoon Granite, Ewen Granite, One Tree Granite, Wills Creek Granite|||
41317|Kalkadoon Suite|69591|5|Briefly described|p31, p34|||Basement rocks in Kalkadoon-Leichhardt Domain, Mount Isa Province.|||Kalkadoon Granodiorite; Ewen, One Tree, Wills Creek Granites; Black Angel, and Pothole, Gneiss Complexes.|Interfingers with Kurbayia Metamorphic Complex.||
41317|Kalkadoon Suite|71341|6|Mentioned|p198|||Mount Isa terrane.||||||
41317|Kalkadoon Suite|72889|5|Briefly described|p1, p9, p14, p17.|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain. A sample of dolerite intruding Kalkadoon Suite rocks yielded an age of 1853.7 +/- 2.9 Ma  which is indistinguishable from Kalkadoon Suite granites and provides direct evidence of coeval mafic and felsic magmatism during the intrusion of the Kalkadoon Suite. Intruded by younger mafic bodies. Contemporaneous with the Leichhardt Volcanics.|c. 1860-1855 Ma.||Includes the Ewen Granite, Kalkadoon Granodiorite.|Intruded by mafic bodies.|Granitic rocks.|25-NOV-20
41317|Kalkadoon Suite|73553|5|Briefly described|p6|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain.|~1850-1865 Ma||Kalkadoon Granodiorite, Ewen Granite, One Tree Granite, Wills Creek Granite||Granitoids.|
30638|Kalkadoon Supersuite|23545|5|Briefly described|p605|||||||||
30638|Kalkadoon Supersuite|24197|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Type example of the Kalkadoon Association. Comprises Kalkadoon Granodiorite, Wills Creek, Woonigan, One Tree, Hardway and Ewen Granites, and Leichardt Volcanics. I-type. Age: ~1860Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
30638|Kalkadoon Supersuite|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Predominantly felsic rocks which form the Kalkadoon-Ewen province.  ||||||
30638|Kalkadoon Supersuite|50332|6|Mentioned|p16|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province. Felsic igneous rocks.||||||07-FEB-11
30638|Kalkadoon Supersuite|50536|5|Briefly described|p2.1|||See also Kalkadoon Suite.||||||
30638|Kalkadoon Supersuite|66302|5|Briefly described|p88|||Mount Isa Province. |||||Granites.|
30638|Kalkadoon Supersuite|66529|6|Mentioned|p67|Paleoproterozoic|Paleoproterozoic||||Includes Ewen Granite and Kalkadoon Granodiorite.|||
30638|Kalkadoon Supersuite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|||Leichhardt River Domain, Mount Isa Inlier.|||Blaze Creek, Plum Mountain Gneisses; Bowlers Hole, Ewen, Hardway, Mairindi Creek, One Tree, Wills Creek, Woonigan Granites; Kalkadoon Granodiorite; Paper Tank Microgranite.||lithology?|
30638|Kalkadoon Supersuite|67779|5|Briefly described|p26.|Paleoproterozoic|Paleoproterozoic|Has strong geochemical and isotopic similarities with the synchronous Nimbuwah Complex.|1867-1862 Ma (Page, 1983).|||||
30638|Kalkadoon Supersuite|68542|6|Mentioned|p1 |||||||||
30638|Kalkadoon Supersuite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
30638|Kalkadoon Supersuite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
30638|Kalkadoon Supersuite|69056|6|Mentioned|p2|||||||||
30638|Kalkadoon Supersuite|69591|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|||||||
30638|Kalkadoon Supersuite|71799|6|Mentioned|p151 fig 3|Orosirian|Orosirian|Mount Isa Region.|ca 1850 Ma|||||
30638|Kalkadoon Supersuite|72889|6|Mentioned|p6 Fig.i.|||||||||
30638|Kalkadoon Supersuite|73137|6|Mentioned|p6, p66|Paleoproterozoic|Paleoproterozoic|Zircons from this unit may be present as inherited grains in a granite of similar age to the Argylla Formation.||||||
30638|Kalkadoon Supersuite|73413|6|Mentioned|p1-2, p5-6, p21-22|Orosirian|Orosirian|Emplaced into basement gneiss of the Kalkadoon-Leichardt Belt. A remnant was identified immediately west of Tick Hill. [Age written as 1860-1850 Ma and 1865-1845 Ma]. [Misspelt as Kalkadoon Supersuit on p22].|1865-1845 Ma||One Tree Granite|||
30638|Kalkadoon Supersuite|73529|6|Mentioned|p15 Fig.11|Orosirian|Orosirian||1870-1860 Ma|||||
30638|Kalkadoon Supersuite|73553|5|Briefly described|p10, p250|Orosirian|Orosirian||1860 Ma||Hardway Granite, Plum Mountain Gneiss|||
75724|Kalkarindji Suite|68193|5|Briefly described|p44|||Kalkarindji Province. Heavily explored, geophysically anomalous locations have all proved negative for diamonds.|||||Basalts.|
75724|Kalkarindji Suite|69417|5|Briefly described|p2:6|Early Cambrian|Early Cambrian|Kalkarindji Province.|507 +/- 4 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69420|6|Mentioned|p5:81|Early Cambrian|Early Cambrian|Covered most of the North Australian Craton.||||||12-JUL-16
75724|Kalkarindji Suite|69422|6|Mentioned|p7:2 Fig.7.2|Cambrian|Cambrian|Kalkarindji Province.||||||12-JUL-16
75724|Kalkarindji Suite|69429|5|Briefly described|p14:4 Fig.14.7|Early Cambrian|Early Cambrian|Kalkarindji Province.|||||Includes basalt flows.|12-JUL-16
75724|Kalkarindji Suite|69432|5|Briefly described|p17:2, 4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Overlies Birrindudu Group.||12-JUL-16
75724|Kalkarindji Suite|69444|6|Mentioned|p29:5-6|||Shares geochemical similarities with the Indiana Suite in the southeastern Harts Range.|c.508 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69445|2|Defined|p30:1-12, 16-17|||Glass and Munson in Ahmad and Munson (2013). New name, after Kalkarindji township. Formerly Kalkarindji Volcanic Group of Kruse in Rawlings et al. (2008). Includes the igneous component of Kalkarindji Large Igneous Province, formerly the Kalkarinji (later revised by Glass and Phillip 2006) Continental Flood Basalt Province of Glass (2002). The definition excludes the minor intercalated sedimentary components of the former Group; they are included within the constituent Formations. 60-1100m thick; 760m thick at the type locality at Purnululu National Park, from WGS84 52K 426414mE 8078661mN to 428989mE 8079851mN. Four reference sections are detailed as are type sections for constituent Formations. Geochemistry and petrology described. Correlated with Mount Wright Volcanics and Cymbric Vale Formation (both Gnalta Group), Truro Volcanics, possibly Mooracoochie Volcanics.|||Antrim Plateau, Helen Springs, Colless, Table Hill Volcanics; Milliwindi Dolerite; Mount Ramsay dolerite.|Unconformably overlies Mount Forster Sandstone. Is overlain unconformably by Headleys, Montejinni, Tindall, Top Springs, Thorntonia Limestones; Tarrara, Gum Ridge, Wonarah Formations.|Tholeiitic basalt and dolerite with massive, porphyritic, partly vesicular (flow tops), amygdaloidal glomeroporphyritic textures, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits.|12-JUL-16
75724|Kalkarindji Suite|69917|6|Mentioned|p175|||Geochemically similar to Coggans Gabbro.|ca 508 Ma|||||
75724|Kalkarindji Suite|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||Includes Antrim Plateau Volcanics, Jindare Formation.|||01-MAR-18
75724|Kalkarindji Suite|70968|5|Briefly described|p6, p51, p100, p131, p137|Early Cambrian|Early Cambrian||||Helen Springs Volcanics.|Unconformably overlies Roper Group.|Basaltic volcanism.|
75724|Kalkarindji Suite|71267|6|Mentioned|1M_geologyp12_lut.csv|||||||||
75724|Kalkarindji Suite|71779|5|Briefly described|p5|Early Cambrian|Early Cambrian|||||Unconformably overlies the Roper Group.||24-SEP-18
75724|Kalkarindji Suite|71893|5|Briefly described|p41, p948|Cambrian|Cambrian|McArthur Basin.|507 +/- 4 Ma (Ar-Ar, Glass and Phillips 2006)|||Overlies the Jamison sandstone.||
75724|Kalkarindji Suite|73083|6|Mentioned|p: 1, 3, 12, 14-15, 17-18, 21, 24-25...|Cambrian|Cambrian|Strongly magnetic. Part of the Kalkarindji Continental Flood Basalt Province. Marked as Ebk on solid geology maps. Widespread in the Georgina Basin sequence. Associated with possible feeder dykes (labelled Ed - Cambrian dolerite) and altered Cambrian basalt is labelled Ebkl. [Written as Kalkarindji Igneous Suite on p30]. More locations p: 28-31, 34-35, 38, 42-45, 48-49, 55.||||Underlain by Kinevans Sandstone.|Basalt and agglomerate.|
24330|Kallala Quartzite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Yaringa Metamorphics. Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
24330|Kallala Quartzite|24419|5|Briefly described|p14, p12 Fig.4, p15 Fig.6|Paleoproterozoic|Paleoproterozoic|Intruded by Sybella Suite granites.  Highly deformed and metamorphosed volcanics and sediments.  Unconformably overlain by Jayah Creek and Oroopa Metabasalts. Geol.Prov: Western Fold Belt, Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
24330|Kallala Quartzite|37862|4|Described|p586|||||||||
24330|Kallala Quartzite|38234|6|Mentioned|Fig.2|||||||||
24330|Kallala Quartzite|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24330|Kallala Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24330|Kallala Quartzite|38658|6|Mentioned|p152|||||||||
24330|Kallala Quartzite|39445|5|Briefly described|Table 2|||||||||
24330|Kallala Quartzite|40840|6|Mentioned|Map legend|||||||||
24330|Kallala Quartzite|41381|6|Mentioned|p325|||||||||
24330|Kallala Quartzite|41978|6|Mentioned|Fig 2 P499|||||||||
24330|Kallala Quartzite|45161|4|Described|p10|||See also P14||||||
24330|Kallala Quartzite|45166|6|Mentioned|p7|||||||||
24330|Kallala Quartzite|49009|2|Defined|p19|Precambrian|Precambrian|Mapped as Eastern Creek Volcanics by Noakes & others (1959).||||||
24330|Kallala Quartzite|49041|5|Briefly described|Table 1|||||||||
24330|Kallala Quartzite|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
24330|Kallala Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartzite; minor amphibolite.||||||
24330|Kallala Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Pre-Barramundi basement to Sybella Domain, Mount Isa Inlier.|||||Quartzite, feldspathic quartzite, minor schist, gneiss|
24330|Kallala Quartzite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, as well as Bucket Hole Metavolcanics, Alpha Centauri Metamorphics and Oroopo Metabasalt, are all mapped under the symbol, -Pvo.||||||25-JUL-13
24330|Kallala Quartzite|69591|5|Briefly described|p29, p58|Paleoproterozoic|Paleoproterozoic|Sybella Domain, Mount Isa Province. |||||Quartzite, feldspathic quartzite, minor schist, gneiss.|
24330|Kallala Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Siliciclastics.|
23679|Kallanda Granite|23422|5|Briefly described|p181, p217 Table 6.11|Carboniferous|Carboniferous|Of Oweenee Supersuite.||||||
23679|Kallanda Granite|23423|5|Briefly described|p252||Carboniferous|Age: 330 +/- 4 Ma.||||||
23679|Kallanda Granite|23431|5|Briefly described|p538|||||||||
23679|Kallanda Granite|23497|6|Mentioned|p30|||of Bedarra belt. Age: 330+/-4 Ma.||||||
23679|Kallanda Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23679|Kallanda Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 135. I-Type.||||||
23679|Kallanda Granite|23617|4|Described|p12 Table 1||Carboniferous|SHRIMP 330 Ma. Also see p22-23 and p52 Table 3. Of Oweenee Supersuite in the Kennedy Province.||||||07-APR-09
23679|Kallanda Granite|23618|5|Briefly described|map legend||Carboniferous|||||||
23679|Kallanda Granite|23893|6|Mentioned|p14|||||||||
23679|Kallanda Granite|24613|6|Mentioned|p108, p113|||Intrudes Ewan Formation and is probably related to extensive tin mineralisation in this unit. Age: 331+/-2Ma (Rb-Sr biotite-total rock).||||||07-FEB-11
23679|Kallanda Granite|42690|5|Briefly described|map legend|Carboniferous||||||||
23679|Kallanda Granite|42692|5|Briefly described|map legend|Carboniferous||||||||
23679|Kallanda Granite|43095|3|Fully described|p54||Early Carboniferous|probable Early Carboniferous age.||||||
23679|Kallanda Granite|43259|4|Described|Appendix 1,p25.||Carboniferous|||||||
23679|Kallanda Granite|43589|2|Defined|p22, p25 appdx.|Early Carboniferous|Early Carboniferous|Age: 330+/-4 Ma (U-Pb Shrimp). Intrudes Running River Metamorphics and Falls Creek Tonalite, Perry Creek and Kangaroo Hills Formations, and Ewan Formation.||||||07-APR-09
23679|Kallanda Granite|60425|5|Briefly described|p98|Early Carboniferous|Early Carboniferous|Of the Oweenie Supersuite. Age: 330+/-4Ma. I-type granite.||||||07-FEB-11
23679|Kallanda Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Has high K, Th and U radiometric responses. Unit in Oweenee Batholith.|||||Pink, orange or cream, fine- to coarse-grained,  porphyritic to seriate biotite granite; common microgranite and abundant greisen and chloritic alteration zones.|
23679|Kallanda Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Has high K, Th and U radiometric responses. Unit in Oweenee Batholith.|||||Pink, orange or cream, fine- to coarse-grained,  porphyritic to seriate biotite granite; common microgranite and abundant greisen and chloritic alteration zones.|
23679|Kallanda Granite|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
23679|Kallanda Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
23679|Kallanda Granite|70207|5|Briefly described|p4-5, p11, p19-24, p28|||NW of Townsville. Unit in the Kennedy Igneous Association. Forms low bouldery outcrops. Previously dated at 330 +/- 4 Ma (U-Pb zircon SHRIMP; Fanning, 1995): possibly two plutons.|340.6 +/- 2.3 Ma (Kositcin et al., 2015).||||Pale pink, medium- to coarse-grained, leucocratic (garnet-)biotite granite.|
23679|Kallanda Granite|71592|5|Briefly described|Appendix A.||||341+/-2.3 Ma (SHRIMP U-Pb zircon).||||Granite.|
37029|Kallee Park Intrusive Complex|23251|6|Mentioned|p39|||Hosts Woolooga Prospect.  See also Kalee Park Intrusive Complex - unclear which spelling is correct?||||||21-JUN-06
36235|Kallon Cauldron Complex|23502|5|Briefly described|Map Legend||Late Carboniferous|of Sundown Volcanic Group.||||||
36235|Kallon Cauldron Complex|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes an un-named unit of flow-banded intrusive rhyolite and porphyritic microgranite.||Unit in Sundown Volcanic Group.|Includes Kallon Volcanics.|||
36235|Kallon Cauldron Complex|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes an un-named unit of flow-banded intrusive rhyolite and porphyritic microgranite.||Unit in Sundown Volcanic Group.|Includes Kallon Volcanics.|||
26649|Kallon Volcanics|23291|4|Described|p38, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Parent: Sundown Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
26649|Kallon Volcanics|23502|5|Briefly described|Map Legend||Late Carboniferous|of Kallon Cauldron Complex, Sundown Volcanic Group.||||||
26649|Kallon Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V88. Assumed to be I-Type.||||||
26649|Kallon Volcanics|23616|5|Briefly described|Table 3 p54||Late Carboniferous|Unconformably overlies Blackman Gap Complex and Proterozoic metamorphic units. Of Sundown Volcanic Group. Dargalong Province. Max thickness ~60 m.||||||
26649|Kallon Volcanics|23624|4|Described|p23|Late Carboniferous|Carboniferous|||||||
26649|Kallon Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26649|Kallon Volcanics|37613|6|Mentioned|p257|||See also Fig.1.||||||
26649|Kallon Volcanics|39445|5|Briefly described|Table 7|||||||||
26649|Kallon Volcanics|42547|5|Briefly described|p74|||||||||
26649|Kallon Volcanics|43259|4|Described|Appendix 1,p8.||Late Carboniferous|||||||
26649|Kallon Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
26649|Kallon Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
26649|Kallon Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
26649|Kallon Volcanics|45014|2|Defined|p52-3,55-6,Pl.38,|Late Carboniferous|Early Carboniferous|Tb.1 (Probably Middle-Late Carboniferous)||||||
26649|Kallon Volcanics|45025|4|Described|p69|Permian|Carboniferous|||||||
26649|Kallon Volcanics|46845|6|Mentioned|Table 1|||||||||
26649|Kallon Volcanics|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Kallon Cauldron Complex.|||Pink to grey, lithics and crystal-rich, rhyodacitic to rhyolitic ignimbrite, porphyritic rhyolite.|
26649|Kallon Volcanics|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Kallon Cauldron Complex.|||Pink to grey, lithics and crystal-rich, rhyodacitic to rhyolitic ignimbrite, porphyritic rhyolite.|
27963|Kalunga Granodiorite|23423|5|Briefly described|p240|||The Silver Pot Granodiorite was previously mapped as part of the Kalunga Granodiorite. Almaden Supersuite.||||||
27963|Kalunga Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Almaden Supersuite. Age: ~299Ma Rb-Sr.||||||
27963|Kalunga Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 255. I-Type.||||||
27963|Kalunga Granodiorite|23616|6|Mentioned|Table 1C p44|||See also p99 Appendix 2.||||||
27963|Kalunga Granodiorite|29820|6|Mentioned|p450|||||||||
27963|Kalunga Granodiorite|32487|6|Mentioned|p15|||||||||
27963|Kalunga Granodiorite|33205|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27963|Kalunga Granodiorite|36527|6|Mentioned|p162|||||||||
27963|Kalunga Granodiorite|39445|6|Mentioned|p90|||Blake(1972)||||||
27963|Kalunga Granodiorite|42547|6|Mentioned|p75|||||||||
27963|Kalunga Granodiorite|43060|5|Briefly described|Table 6|||of Almaden Supersuite||||||
27963|Kalunga Granodiorite|43259|4|Described|Appendix 1,p34.||Late Carboniferous|Late? Carboniferous.||||||
27963|Kalunga Granodiorite|45065|4|Described|Table 4|||||||||
27963|Kalunga Granodiorite|45113|3|Fully described|p15|||Emphasis on petrography.||||||
27963|Kalunga Granodiorite|46879|6|Mentioned|Fig.1|||||||||
27963|Kalunga Granodiorite|48976|4|Described|p42|||Isotopic data Table 10||||||
27963|Kalunga Granodiorite|60425|4|Described|p45 Tb. 3, p74, p282-3 Appdx.|Early Permian|Early Permian|Of Kalunga Suite (Almaden Supersuite). Unconformably overlain by/or intruded by Slaughter Yard Creek Volcanics. Part of this unit remapped as Silver Pot Granodiorite (Champion and Heninemann 1994). Lith. details included for this granodiorite. I-type||||||07-FEB-11
30428|Kalunga Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite (Almaden Supersuite).||||||15-JUN-06
30428|Kalunga Suite|60425|5|Briefly described|p282-3 Appdx.|Early Permian|Late Carboniferous|Of Almaden Supersuite.  Contains 3 granodiorites, namely, Bakerville, Kalunga and Poona Creek Granodiorites. I-type.||||||07-FEB-11
31447|Kandanga Creek Megabreccia|22845|2|Defined|p33,70-2,79|Triassic|Late Carboniferous|After Sliwa 1994 formerly (Murphy 1976) part of the Neara Volcanics||||||
31447|Kandanga Creek Megabreccia|22846|6|Mentioned|p41|||||||||
31447|Kandanga Creek Megabreccia|43588|6|Mentioned|p301||Late Devonian|||||||
31447|Kandanga Creek Megabreccia|44923|5|Briefly described|Map Legend||Permian|||||||
31447|Kandanga Creek Megabreccia|50320|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Marumba Subprovince (Wandilla Province)||||||
31447|Kandanga Creek Megabreccia|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with the Marumba, Northbrook and Cambroon beds, and the Cedarton Volcanics, are all mapped under the symbol, Pn.||||||
31447|Kandanga Creek Megabreccia|68679|5|Briefly described|p324-326, p384, p387|Permian|Permian|Sliwa (1994). Cressbrook Basin, northern New England Orogen. Is exposed in two small areas (total area <10 km2) and 5km apart along Kandanga Creek. Cover basin sediments. Contains late Pennsylvanian (?Gallangowan) granodiorite boulders.||||Is faulted against Amamoor beds and Mount Mia Serpentinite. Is overlain unconformably by Neara Volcanics. Probably correlates with Marumba and Cambroon beds and Cedarton Volcanics.|Eastern unit: matrix-supported conglomerate with angular to subrounded blocks to 10m; minor pebble to cobble conglomerate. Western unit: clay matrix-supported, poorly-sorted cobble (mainly) conglomerate with boulders to 1.3m.|
32139|Kandoonan Granite|23037|6|Mentioned|p83|Early Permian|Silesian|||||||
32139|Kandoonan Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgkd].  Pink to grey, medium-grained hornblende?-biotite granite.||||||
32139|Kandoonan Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to grey, medium-grained, hornblende-biotite granite.||||||
32139|Kandoonan Granite|65388|4|Described|p262, p236 Fig. 81, p237, 238|Early Permian|Late Carboniferous|Has hornfelsed the Torsdale Volcanics. Relationship to Hainault Granodiorite is unclear. Age tentative. Outcrop poor. Grey to pink, medium-grained hornblende-biotite granite. ||||||
32139|Kandoonan Granite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Torsdale Volcanics.|Grey to pink, medium-grained granite.|
36282|Kangaroo Creek Supersuite|23291|4|Described|p46, p97 Tb. 3.11|Early Permian|Early Permian|Geological Province: Georgetown Region.||||||08-JUL-15
36282|Kangaroo Creek Supersuite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36282|Kangaroo Creek Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Brodies Camp, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36282|Kangaroo Creek Supersuite|69593|4|Described|p484-485, p487, p489|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. In the vicinity of, and intruding, Galloway Volcanic Group. Outcrop area ~100 km2. Early Permian.|~290-280 Ma.||Bull Creek, Campbell Mountain, Copper Bush, Promise Creek Granites.|Intrudes Galloway Volcanic Group.|A-type. Biotite and biotite-hornblende granite and microgranite, hornblende-biotite and biotite granodiorite; microtonalite as rafts within the granites.|
77803|Kangaroo Rat Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Topaz-muscovite-biotite granite.|19-MAR-13
82989|Kangerong Basalt|73115|6|Mentioned|p76-77, 87, 90, 94, 99, 105,110,115,120|Pleistocene|Pleistocene|Nulla Basalt Province. Interbedded with Campapse [Campaspe] Formation.|2.4-2.3 Ma|||||
36208|Kangerong Basalt Flow|23509|5|Briefly described|Map Legend|Quaternary|Tertiary|Informal name.||||||
36208|Kangerong Basalt Flow|43933|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
36208|Kangerong Basalt Flow|69789|5|Briefly described|p1045|Pliocene|Pliocene|Appears as Kangerong flow. Occupies an incision on Campaspe Formation surface.|2.4 Ma (K-Ar); Wyatt and Webb, 1970.|||||
70402|Kantaka Monzogranite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Medium-grained slightly porphyritic biotite monzogranite with common enclaves of microdiorite and metamorphic biotite gneiss.|
27171|Karana Quartz Diorite|35812|2|Defined|p568|Middle Triassic|Middle Triassic|||||||
27171|Karana Quartz Diorite|35866|6|Mentioned|p402|||||||||
27171|Karana Quartz Diorite|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
27171|Karana Quartz Diorite|36779|5|Briefly described|p6|||||||||
27171|Karana Quartz Diorite|36937|6|Mentioned|p229|||||||||
27171|Karana Quartz Diorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
27171|Karana Quartz Diorite|38074|6|Mentioned|Table 2|||||||||
27171|Karana Quartz Diorite|39079|6|Mentioned|p9|||||||||
27171|Karana Quartz Diorite|40623|5|Briefly described|p30|||||||||
27171|Karana Quartz Diorite|41906|5|Briefly described|p12|||||||||
27171|Karana Quartz Diorite|43008|5|Briefly described|map legend|||||||||
27171|Karana Quartz Diorite|43009|5|Briefly described|Map Legend|||||||||
27171|Karana Quartz Diorite|43076|5|Briefly described|p6|||||||||
27171|Karana Quartz Diorite|68576|5|Briefly described|QLD_D1: p3|||Mount Crosby. Used in the base course and plinth in the Old Administration Building; steps and base of the Queen Victoria statue in Queens Park.|||||Dark grey diorite.|
31365|Karandah Granodiorite|23251|6|Mentioned|p29|||of Crouch and others (1995). Synkinematic S-type granitoid.||||||
31365|Karandah Granodiorite|23608|4|Described|p50 Fig 1, p51 Fig 3.||Carboniferous|Transitional S- to I-type granite.  Of Wratten Igneous Suite. North D'Aguilar Block.||||||
31365|Karandah Granodiorite|23609|5|Briefly described|p7|||Also see Fig 1 p6 and p9. North D'Aguilar Block.||||||
31365|Karandah Granodiorite|23799|5|Briefly described|p23, p123|Late Carboniferous|Late Carboniferous|Geological Province:  North D'Aguilar Subprovince.||||||
31365|Karandah Granodiorite|24382|5|Briefly described|Map legend|Carboniferous|Carboniferous|||||||17-OCT-12
31365|Karandah Granodiorite|43588|6|Mentioned|p30||Late Carboniferous|Variation on Karandah Adamellite||||||
31365|Karandah Granodiorite|44923|5|Briefly described|Map Legend||Carboniferous|||||||
31365|Karandah Granodiorite|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
31365|Karandah Granodiorite|63821|5|Briefly described|p27|Late Carboniferous|Late Carboniferous|Intrudes Curtis Island Group. Part of a suite of S-type granitoids. Foliated biotite granodiorite.||||||07-FEB-11
31365|Karandah Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Capsize Creek Complex; the Coppermine Creek, Gallangowan, Claddagh and Yabba Creek Granodiorites, are all mapped under the same symbol, Cgd.||||||
31365|Karandah Granodiorite|68679|5|Briefly described|p312,p320,p323, p325-326, p331, p403-405|Carboniferous|Carboniferous|Kilkivan-Manumbar area, North D'Aguilar Subprovince, Northern New England Orogen. Syntectonic granitoid.||Wratten Igneous Suite.|||Coarse-grained, foliated biotite granodiorite; early crystals plastically deformed; cataclastic material strongly foliated.|
22067|Kariboe Layered Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgka].  Layered gabbro, diorite, tonalite and minor hornblendite.||||||
22067|Kariboe Layered Gabbro|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||14-MAY-04
22067|Kariboe Layered Gabbro|60282|6|Mentioned|p20, p22|||See also Kariboe Gabbro.  Names used interchangeably.||||||13-APR-05
22067|Kariboe Layered Gabbro|65388|3|Fully described|p322-323, 294,  p301 Fig 98, p338|Early Triassic|Late Permian|One of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton. Has metamorphosed Lochenbar Formation.  In contact with Wingfield Granite. Relationship uncertain. Layered gabbro including ferrigabbro, olivine gabbro, hypersthene gabbro, and porphyritic augite gabbro. Also includes hornblende gabbro to diorite and tonalite, quartz monzogabbro to diorite and rare hornblendite. Hosts Cu mineralisation.||||||
22067|Kariboe Layered Gabbro|68008|6|Mentioned|p67, p432|||Bellamy (1976). This name seems to be used interchangeably with Kariboe Layered Gabbro Intrusion (the original form) and Kariboe Gabbro.||||||
22067|Kariboe Layered Gabbro|68679|5|Briefly described|p416-417, p419|||Far north of the Rawbelle Batholith. ~20 km2.||||Intrudes Lochenbar Formation.|Layered gabbro, diorite, tonalite and minor hornblendite; ferrogabbro, olivine gabbro, hypersthene gabbro and porphyritic augite gabbro zones; exhibits centimetre-scale layering locally appearing cross-bedded.|
23688|Karmoo Quartz Diorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37.||||||
23688|Karmoo Quartz Diorite|43029|2|Defined|p18||Middle Devonian|Rb-Sr age of 384 Ma,see also Fig.2,p16||||||
23688|Karmoo Quartz Diorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
23688|Karmoo Quartz Diorite|43213|3|Fully described|p96-97, p104-105, p116-121, p174-175|Middle Devonian|Middle Devonian|See also p179, p208, p211, p215-217, p231, p240. Type area described. Component of the Retreat Batholith. Rb-Sr biotite-whole rock pair age by Carr (pers.comm.), 1993. Peraluminous. Geochemistry, modal analyses and geophysics detailed.|384 +/- 3 Ma.|||Intrudes Anakie Metamorphic Group. Is faulted against Kilmarnock Granodiorite.|A composite pluton of grey, fine- to medium-grained, equigranular, biotite-hornblende quartz diorite and tonalite with subordinate hornblende-biotite granodiorite, biotite-hornblende diorite, hornblende gabbro and rare biotite granodiorite.|
23688|Karmoo Quartz Diorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||384+/-3 Ma, Rb-Sr biotite||||Grey, fine to medium-grained, biotite-hornblende quartz diorite and tonalite with subordinate hornblende-biotite granodiorite and biotite-hornblende diorite or gabbro; locally abundant xenoliths and pendants of country rocks.|01-SEP-14
23688|Karmoo Quartz Diorite|68731|6|Mentioned|p132|||||||||
82214|Karungle Volcanics|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Andesite, dacite?, rhyolite (commonly flow banded and locally autobrecciated), volcanic breccia, tuff, polymictic conglomerate.|
36175|Kauri Granite|23506|5|Briefly described|Map Legend||Early Permian|of O'Briens Creek Supersuite.||||||
36175|Kauri Granite|60425|4|Described|p284-5 Appdx.|Early Permian|Early Permian|Of Cherry Tree Suite (O'Briens Creek Sup'suite).Extensively altered.Detailed lithol.included; I-type.Delineated as discrete unit and named Nigger Creek granite by Clarke (1990, 1995); included in Saint Patrick Hill Granite by Donchak and Bultitude (1998).||||||07-FEB-11
76901|Kays Peak Granite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event||Williams Supersuite|||Coarse-grained muscovite-biotite granite|
76901|Kays Peak Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Coarse-grained muscovite-biotite granite.|
76901|Kays Peak Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Coarse-grained muscovite-biotite granite.|05-MAY-16
76901|Kays Peak Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Coarse grained muscovite-biotite granite.
|
76901|Kays Peak Granite|71592|5|Briefly described|Appendix A.|||Soldiers Cap Domain, Mount Isa Orogen.|1536+/-20 Ma (U-Pb zircon SHRIMP)||||Granite.|
80675|Keane Granite|71849|3|Fully described|p8, p14, p65-67, p116, p119, p149|Devonian|Devonian|See also p155-157, p195. New name, after the Parish of Keane. Previously mapped as part of Kintore Adamellite and Flyspeck Granodiorite by various authors (listed). An irregular, horseshoe-shaped body ~27-35km NW of Coen. Very poorly exposed as scattered bouldery rubble. Type area is around MGA 711609 8482654. Geophysics described briefly; geochemistry in more detail. Not isotopically dated. Member of Pama Igneous Association.||Ebagoola Suite.||(Interpreted to) intrude Rokeby Quartz Monzodiorite.|Pale grey, fine- to medium-grained, slightly porphyritic muscovite-biotite monzogranite. Peraluminous, calc-alkaline S-type.|
80675|Keane Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Pale grey, fine- to medium-grained, slightly porphyritic muscovite-biotite monzogranite.|
80675|Keane Granite|73387|6|Mentioned|p29|||S-type.||Kintore Supersuite||Intrudes Rokeby Quartz Monzodiorite.||
30011|Keating Granodiorite|23511|5|Briefly described|Map Legend||Late Permian|of Yates Supersuite.||||||
30011|Keating Granodiorite|43070|2|Defined|p78|Late Permian||Of Yates Supersuite.||||||03-JUN-09
30011|Keating Granodiorite|43285|5|Briefly described|Map Legend||Late Permian|||||||
30011|Keating Granodiorite|43625|5|Briefly described|p128,Appendix 8|||||||||
30011|Keating Granodiorite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Yates Supersuite.  Slightly porphyritic, biotite granodiorite to granite.||||||
30011|Keating Granodiorite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Keating Suite (Yates Supersuite). I-type. White to grey, fine to medium-grained, slightly  porphyritic Biotite granodiorite to granite?; scattered mafic enclaves to 30cm. Accessory apatite, zircon, ilmenite, tourmaline, titanite.||||||07-FEB-11
30011|Keating Granodiorite|69593|5|Briefly described|p480, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.  Sm-Nd isotope data tabulated.|260 Ma.|Yates Supersuite.|||I-type.|
30113|Kedumba Granodiorite|22847|3|Fully described|p 53|Early Devonian|Late Silurian|||||||
30113|Kedumba Granodiorite|23422|5|Briefly described|p176, p214 Table 6.8|||Of Barrabas Supersuite.||||||
30113|Kedumba Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
30113|Kedumba Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 483. I-Type.||||||
30113|Kedumba Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|Variation on reserved name Kedumba Complex?||||||
30113|Kedumba Granodiorite|43259|4|Described|Appendix 1,p51.|Early Devonian|Late Silurian|||||||
30113|Kedumba Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
30113|Kedumba Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Kedumba gdrt.||Unit in Barrabas Supersuite.||||
30113|Kedumba Granodiorite|64852|5|Briefly described|Map legend|Devonian|Silurian|Pinkish grey, medium-grained, hornblende-biotite granodiorite (with sparse 1cm hornblende phenocrysts).||||||
30113|Kedumba Granodiorite|69592|5|Briefly described|p293|||Southeast Ravenswood Batholith, Charters Towers Province.||Barrabas Supersuite.|||High-K and high-Rb granitoids.|
30113|Kedumba Granodiorite|70740|5|Briefly described|p40, p41|||Outcrop characteristics discussed. A type area is mentioned and described. Petrography in the type area is described. Intruded by a number of unnamed gabbro and diorite plugs.||Barrabas Supersuite||Overlain by the Mount Cuthbert Granodiorite.|Pinkish-grey, medium-grained, hornblende-biotite granodiorite.|
27810|Keelbottom Group|22800|5|Briefly described|Fig.14 p591, 592|Tournaisian|Famennian|||||||
27810|Keelbottom Group|23422|4|Described|p180|Early Carboniferous|Late Devonian|Overlain by Glenrock Group. Underlain by Dotswood Group. Maximum thickness: 2590m. Geological Province: Burdekin Basin.||||||14-NOV-07
27810|Keelbottom Group|23430|5|Briefly described|p506|||Underlain by Dotswood Group. Burdekin Basin Province.||||||23-APR-08
27810|Keelbottom Group|23431|5|Briefly described|p538|||Burdekin Basin Province.||||||
27810|Keelbottom Group|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
27810|Keelbottom Group|23522|5|Briefly described|p259|Late Devonian|Late Devonian|||||||
27810|Keelbottom Group|23893|5|Briefly described|p16|Tournaisian|Famennian|Geological Province: Burdekin Province.||||||
27810|Keelbottom Group|24577|5|Briefly described|p755 Fig. 2|Carboniferous|Carboniferous|Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
27810|Keelbottom Group|24610|5|Briefly described|p62|||Geological Province: Burdekin Basin.||||||
27810|Keelbottom Group|24611|5|Briefly described|p194|Early Carboniferous|Late Devonian|Overlies Mount Podge Limestone.  See also p194 Fig. 1.||||||
27810|Keelbottom Group|24612|5|Briefly described|p7, p9 Fig.2|Early Carboniferous|Late Devonian|Geological Province: Burdekin Basin.||||||
27810|Keelbottom Group|24613|2|Defined|p3, p6 Fig. 6, p61|Early Carboniferous|Late Devonian|Formerly "Star Series", Star Beds. Incl: Myrtlevale, Lollypop, Hardwick+Piccadilly Fms. Conform.on Dotswood Gp, unconform.on Fanning Riv.Gp elsewhere; unconform.on Argentine Metamorphics (Star River area); unconform.below Glenrock Group. Max.thick:2590m||||||07-FEB-11
27810|Keelbottom Group|24614|4|Described|p191 Fig. 1, p195|Tournaisian|Famennian|Includes Myrtlevale, Lollypop, Hardwick and Piccadilly Formations. Conformably overlies the Dotswood Group; unconformably overlies the Burdekin Limestone at Mount Podge; also overlies Argentina Metamorphics at Star homestead. Geol Prov: Burdekin Basin.||||||15-JUL-14
27810|Keelbottom Group|31999|6|Mentioned|p141|||||||||
27810|Keelbottom Group|37565|6|Mentioned|Fig.8|||||||||
27810|Keelbottom Group|37573|4|Described|p216|||See also Fig.2.||||||
27810|Keelbottom Group|39445|6|Mentioned|p80|||See also Table 6||||||
27810|Keelbottom Group|39686|6|Mentioned|Fig.1|||||||||
27810|Keelbottom Group|40623|5|Briefly described|p88|||||||||
27810|Keelbottom Group|41735|6|Mentioned|p284|||||||||
27810|Keelbottom Group|41774|6|Mentioned|p31|||||||||
27810|Keelbottom Group|42295|5|Briefly described|Fig.2 P5|||||||||
27810|Keelbottom Group|42407|6|Mentioned|p13|||Formerly Star beds||||||
27810|Keelbottom Group|42547|5|Briefly described|p66|||||||||
27810|Keelbottom Group|42689|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27810|Keelbottom Group|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27810|Keelbottom Group|42692|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
27810|Keelbottom Group|42750|6|Mentioned|p46|||||||||
27810|Keelbottom Group|42933|5|Briefly described|p154|||||||||
27810|Keelbottom Group|43095|5|Briefly described|Plate 2|||||||||
27810|Keelbottom Group|43589|6|Mentioned|p22|Early Carboniferous|Late Devonian|Intruded by Spinifex Creek Granite.||||||23-APR-08
27810|Keelbottom Group|43933|5|Briefly described|Map Legend|Carboniferous|Late Devonian|||||||
27810|Keelbottom Group|62522|5|Briefly described|p20|||Undifferentiated parts of this group overlie Kukiandra Formation conformably. Geological Province: Burdekin Basin.||||||
27810|Keelbottom Group|63154|5|Briefly described|p285 Fig. 5|Devonian|Devonian|Geological province: Charters Towers Province. Mixed shallow marine sediments.||||||
27810|Keelbottom Group|66529|5|Briefly described|p24 |Early Carboniferous|Late Devonian|||||Overlain by the Saint James Volcanics.||
27810|Keelbottom Group|67402|5|Briefly described|p246|Tournaisian|Famennian|Burdekin Basin. |||Includes the Myrtlevale Formation, Lollypop Formation, Hardwick Formation and the Piccadilly Formation.|Overlies the Dotswood Group.||
27810|Keelbottom Group|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.|||Includes Myrtlevale, Lollypop and Hardwick Formations.|||
27810|Keelbottom Group|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.|||Includes Myrtlevale, Lollypop and Hardwick Formations.|||
27810|Keelbottom Group|68419|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.|||Includes Piccadilly, Hardwick, Lollypop and Myrtlevale Formations.|Shown as older than the Glenrock Group.|Undivided: mudstone, quartzose and feldspathic to lithic sandstone (locally calcareous), fossiliferous sandy limestone and calcilutite, basal quartzose conglomerate and sandstone.|
27810|Keelbottom Group|68420|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.|||Includes Piccadilly, Hardwick, Lollypop and Myrtlevale Formations.|Shown as older than the Glenrock Group.|Undivided: mudstone, quartzose and feldspathic to lithic sandstone (locally calcareous), fossiliferous sandy limestone and calcilutite, basal quartzose conglomerate and sandstone.|
27810|Keelbottom Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Burdekin Basin.||||||
27810|Keelbottom Group|68731|5|Briefly described|p183, p185 Tb 3.4, p186, p187|Mississippian||Burdekin Basin. Characterised by shallow-marine intervals interlayered with terrestrial strata (Gunther, Lang and Draper 1990a). A siliciclastic component to sand size is characteristic.|||Includes the Piccadilly Formation, Hardwick Formation, Lollypop Formation, and Myrtlevale Formation.|Unconformably overlain by the Percy Creek Volcanics and the Glenrock Group. Disconformably overlain by the Tareela Volcanics.|Siliciclastic, predominantly fluviatile, but thin, shallow, marine intercalations also occur.|15-JUL-14
27810|Keelbottom Group|70207|6|Mentioned|p20|Early Carboniferous|Late Devonian|Clarke River and/or Cairns region.||||||
32140|Keen Creek Granite|23037|5|Briefly described|p85|Early Permian|Silesian|||||||
32140|Keen Creek Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgkc].  Grey, fine- to medium-grained biotite granite.||||||
32140|Keen Creek Granite|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32140|Keen Creek Granite|65388|3|Fully described|p263, p236 Fig. 81, p237, 238, 272|Early Permian|Late Carboniferous|Appears to intrude the Pinedale Granite mainly on the basis of the shape of its contact as mapped from the radiometric data. It is intruded by the Montour Gabbro. Age tentative. Pale grey to pale pink, fine to medium-grained biotite granite. Poor outcrop. Deeply weathered & capped by duricrust.||||||
32140|Keen Creek Granite|68679|5|Briefly described|p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Pinedale Granite. Is intruded by Montour Gabbro.|Pale grey to pale pink, fine- to medium-grained biotite granite.|
30700|Keithys Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30700|Keithys Granite|50536|5|Briefly described|p1.5, 8.1, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite. Age: 1671-1688 +/- 23Ma (U-Pb).||||||07-NOV-08
30700|Keithys Granite|63023|6|Mentioned|p1037 Fig, 9|Paleoproterozoic|Paleoproterozoic|Age range: ~1680-1665Ma. ||||||07-NOV-08
30700|Keithys Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p12|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl. Sybella Domain, Mount Isa Inlier. Sybella Igneous Event. Exhibits NW trending linear fabric (Keithy pluton, Keithy Granite p12)|1671 +/- 8 Ma.|Sybella Suite.|||Medium- to coarse-grained, slightly porphyritic biotite granite, microgranite.|
30700|Keithys Granite|69591|5|Briefly described|p59|||Sybella Batholith.|1671 +/- 8 Ma (Page and Bell, 1986).||||Medium- to coarse-grained slightly porphyritic biotite granite, microgranite.|
30700|Keithys Granite|71592|5|Briefly described|Appendix A.|||Sybella Domain, Mount Isa Orogen.|1671+/-8 Ma (crystallisation: U-Pb zircon TIMS).||||Granite.|
36718|Kelly Saint George Granite|23423|6|Mentioned|p238|||Written as Kelly St George Granite.||||||
36718|Kelly Saint George Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province.||||||02-JUN-09
36718|Kelly Saint George Granite|60425|4|Described|p72, p81, p190, p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla S'suite). Age: 280-275Ma (est.) Rb-Sr). S-type.Musc.-biotite granite+scattered gneiss+qtz enclaves; pronounced NW'ly and N'ly elongations; +miarolitic cavities - lith.details incl'd. In Kennedy Province. Saint is St in text||||||07-FEB-11
36718|Kelly Saint George Granite|66852|5|Briefly described|pp937-938.|||Written as Kelly St George Granite in article. Shows evidence of syntectonic emplacement. ||Unit in Whypalla Supersuite.||||
36718|Kelly Saint George Granite|69592|5|Briefly described|p247-248, p249 Fig.4.34|||Western Palmer-Barron Subprovince. Photograph of deformation fabric in aureole.||||Intrudes Hodgkinson Formation.||
36718|Kelly Saint George Granite|69593|5|Briefly described|p479, p481 Fig.6.4, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 Ma.|Curraghmore Suite.|||S-type.|15-MAR-23
25115|Kendall Surface|37605|5|Briefly described|p380|||||||||
25115|Kendall Surface|37607|5|Briefly described|Fig.3|||See also P333 and P335.||||||
25115|Kendall Surface|39556|5|Briefly described|Map legend|Pliocene|Pliocene|||||||
25115|Kendall Surface|39562|5|Briefly described|Map legend|Pliocene|Pliocene|Duricrust-ferricrete, commonly with thin sand cover.||||||15-JUN-06
25115|Kendall Surface|39899|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
25115|Kendall Surface|40000|6|Mentioned|p254|||||||||
25115|Kendall Surface|42650|5|Briefly described|p18|||||||||
25115|Kendall Surface|69599|5|Briefly described|p584-586, p603, p651|Pliocene|Pliocene|Gulf of Carpentaria lowlands and Cape York Peninsula. Lateritisation of the Wyaaba beds. May be coeval with the Campaspe Surface.||||||
25115|Kendall Surface|70352|5|Briefly described|Map legend|Neogene|Neogene||||||Deeply weathered: ferricrete and minor silcrete.|
25115|Kendall Surface|70570|5|Briefly described|Map legend.|Neogene|Paleogene|Deeply weathered.|||||Ferricrete and minor silcrete.|
23693|Kendle River Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Lankelly Suite||||||
23693|Kendle River Granite|22781|4|Described|p30|Paleozoic|Paleozoic|Lankelly Suite||||||07-NOV-08
23693|Kendle River Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Lankelly Suite of the Kintore Supersuite. Intrudes Coen Metamorphic Group.||||||
23693|Kendle River Granite|42610|2|Defined|p19|Early Devonian|Early Devonian|Age assumed similar to Lankelly & Kintore Granites - 400Ma.||||||
23693|Kendle River Granite|43738|6|Mentioned|Fig.12,p38|||||||||
23693|Kendle River Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
23693|Kendle River Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Lankelly Suite.|||Pale grey, variably porphyritic to megacrystic muscovite-biotite granite.|
33722|Kenewah Granodiorite|23799|3|Fully described|p77, p14 Tb. 1|Triassic|Permian|Originally mapped as Woolshed Mountain Granodiorite (Cranfield & Schwarzbock, 1974).  Intrudes the Sugarloaf Metamorphics.  Of the South-east Queensland Volcanic and Plutonic Intrusives.||||||
33722|Kenewah Granodiorite|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
33722|Kenewah Granodiorite|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||
33722|Kenewah Granodiorite|60370|5|Briefly described|Map Legend|Triassic|Permian|Medium to coarse biotite granodiorite, granite||||||
33722|Kenewah Granodiorite|68679|5|Briefly described|p413-414|||Separated from the Woolshed Mountain Granodiorite on geophysical responses.||||Adjacent to Djuan Tonalite.|Grey and pink, equigranular to moderately porphyritic, biotite-hornblende granodiorite; lesser grey-pink, medium, sparsely porphyritic biotite granite.|
69840|Kenilworth Bluff Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
69840|Kenilworth Bluff Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Rhyolitic tuff.|
41266|Kenmore Gabbro|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium grained biotite-hornblende gabbro.||||||30-JUN-04
41266|Kenmore Gabbro|65388|3|Fully described|p323, p301 Fig 98|Early Triassic|Late Permian|Intrudes Narayen beds. Overlain by Evergreen Formation. Age uncertain. Dark bluish grey to greenish grey, fine to medium-grained gabbro. Poor outcrop.||||||
41266|Kenmore Gabbro|68679|5|Briefly described|p419|||A circular, 1.5 km diameter intrusion in the Rawbelle Batholith.||||Intrudes Narayen beds.|Biotite-hornblende gabbro.|
80561|Kennedy Hill Granite|71792|4|Described|p33, p43-p45|Early Permian|Early Permian|Northern Coen Inlier. Named for the Kennedy Hill. No type area has been assigned. Outcrops in a large area along the coast between the Pascoe River mouth in the south and First Stony Point in the north. The unit is roughly ovoid in shape. Rocks of this unit were previously mapped as parts of unnamed unit Ph and Weymouth Granite (Willmott et al, 1973) but is now interpeted as a separate unit on the basis of its radiometrics response. The distribution of this unit has been defined in Geophysics (radiometrics and magnetic response discussed). Modern alluvial sediments in drainages emanating from this unit host cassiterite in the northern and southern extremities of the unit. The cassiterite is interpreted to derive from the fractionated granite and associated pegmatite veins.||||Intrudes (or appears to) the Weymouth Granite and the Kangaroo River Volcanics.|Medium- or coarse-grained leucocratic biotite-hornblende granite.|10-AUG-18
80561|Kennedy Hill Granite|71853|5|Briefly described|Map legend.|Permian|Permian|The two facies are mapped separately.|||||Medium- or coarse-grained, leucocratic biotite-hornblende granite; deeply weathered granite.|
37278|Kent Island serpentinite|24003|6|Mentioned|p256 Fig.1|||Informal name||||||
28642|Kerosene Creek Member|39493|2|Defined|p94|late Eocene|middle Eocene|Mid to late Eocene||||||
28642|Kerosene Creek Member|39997|6|Mentioned|p165|||||||||
28642|Kerosene Creek Member|40116|6|Mentioned|p29|||||||||
28642|Kerosene Creek Member|41927|4|Described|p66|||||||||
28642|Kerosene Creek Member|42021|4|Described|p321|||See also Fig.5 and 6||||||
28642|Kerosene Creek Member|71092|5|Briefly described|p232-233|Eocene|Eocene|Crocodilian and turtle fossils. Systematic palaeontology descriptions.||Topmost Rundle Formation.||||
28642|Kerosene Creek Member|72297|5|Briefly described|p752-753|||Narrows Graben. During 1999-2004, a demonstration-scale shale oil processing plant at the Stuart deposit near Gladstone produced 4500 barrels per day from 6000 t/d; more details given.||Rundle Formation.||||
22089|Kettle Conglomerate Member|43204|5|Briefly described|Map Legend|Early Permian|Early Permian|Denison Trough, Bowen Basin||Aldebaran Sandstone||||23-DEC-11
22089|Kettle Conglomerate Member|43213|5|Briefly described|p154, p239|||Grimes et al. (1980), for a sequence of sediments informally called the "Kettle beds" by Robertson (1974). The quartz and quartz sandstone clasts were derived from Mount Hall Formation, various units in the Retreat Batholith, and the Anakie Metamorphic Group.||Unit in Aldebaran Sandstone.|||Cross-bedded, pebbly, quartzose sandstone and conglomerate.|
22089|Kettle Conglomerate Member|60369|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Aldebaran Sandstone. Unconformably overlies Retreat Granite. Quartz pebble conglomerate, quartz sandstone.||||||02-SEP-04
22089|Kettle Conglomerate Member|69599|5|Briefly described|p593|Permian|Permian|||Aldebaran Sandstone.||||
75659|Key Creek Gneiss|67874|6|Mentioned|p50|||Mentioned in analytical session metadata.||||||
75659|Key Creek Gneiss|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Connors Subprovince. This unit, as well as the Mount Cavana beds and Inkerman Metamorphics, are all mapped under the symbol, DCi.||||||
75659|Key Creek Gneiss|68679|5|Briefly described|p347, p360-362, p364, p368-369|Carboniferous|Late Devonian|A previously unrecognised metamorphic complex ~65km SSW of Bowen. Crops out over ~265 km2 in the middle of the Urannah Batholith. Northern New England Orogen. May represent an extensional core complex; discussed. Zircons and monazites record  a significant high-grade metamorphic event or events at ~298-291 Ma; several age determinations (U-Pb SHRIMP or ID-TIMS: Cross et al. 2012) elaborated on p362.|292.5 +/- 1.8 Ma metamorphic age.||||Mainly low-P high-T, upper amphibolite grade biotite gneisses and migmatitic gneisses; distinctive elevated Th response on radiometric images; has shallow-dipping foliation in many places.|
75659|Key Creek Gneiss|68901|5|Briefly described|p2-p3, p4, p28-p43, p144|Carboniferous|Late Devonian|northern New England Orogen, Bowen Region. Occurs roughly in the centre of the Urannah Batholith. 3 samples dated. Metamorphism dated by ID-TIMS and U-Pb monazite analyses at 298 to 291 Ma. An additional metamorphic age of 297 +/- 2.7 Ma is also given. Maximum depositional age of 328+/-8 Ma given on p30. Maximum depositional age of second sample: 319+/-12 Ma (p38). Magmatic crystallisation age of leucotonalite lens sample: 292.5+/-1.8 Ma.|291 +/- 0.9 Ma (ID-TIMS monazite, Metamorphism)|||leucotonalite lens same age as East Creek Tonalite.|Upper amphibolite grade paragneiss with a distinctive elevated Th response.|28-SEP-18
75659|Key Creek Gneiss|69952|5|Briefly described|p85-86|Carboniferous|Late Devonian|Two metamorphic ages, 297.0 +/- 2.7 Ma and 298.2 +/- 6.9 Ma (Cross et al., 2012), are within error of the age of the adjacent Pickhandle Tonalite (297.1 +/- 2.0 Ma), implying granitoid emplacement and metamorphism were part of the same event.||||Adjacent to Pickhandle Tonalite.||
75659|Key Creek Gneiss|70673|5|Briefly described|p6, p8-9, p134-137|||An extensive metamorphic complex in the centre of the Urannah Batholith, Bowen hinterland. This age determination (this study) supports an ID-TIMS monazite age of 291.0 +/- 0.9 Ma (Cross et al., 2012) which was younger than previous determinations (described).|288.3 +/- 3.7 Ma (SHRIMP monazite age).||||Upper-amphibolite grade paragneisses.|
75659|Key Creek Gneiss|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen. Metamorphosed at 297 +/- 2.7 Ma (U-Pb zircon SHRIMP).|319+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Gneiss, tonalite.|
75659|Key Creek Gneiss|73036|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous||||||Dark grey, fine to medium-grained, slightly uneven-grained muscovite-biotite gneiss and migmatitic gneiss; with small andalusite porphyroblasts, minor garnet, and traces of sillimanite (fibrolite); commonly with boudins of quartz and metagreywacke(?)|
26661|Kholo Subgroup|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Ipswich Coal Measures|Includes Blackwall Breccia, Mount Crosby Volcanics, Colleges Conglomerate, Hector Tuff, Cribb Conglomerate|||
26661|Kholo Subgroup|35812|6|Mentioned|p570|||||||||
26661|Kholo Subgroup|36243|6|Mentioned|p74|||See also Table 10A.||||||
26661|Kholo Subgroup|36351|6|Mentioned|p373|||||||||
26661|Kholo Subgroup|36354|6|Mentioned|Fig.1|||||||||
26661|Kholo Subgroup|38306|6|Mentioned|p512|||||||||
26661|Kholo Subgroup|38307|6|Mentioned|p519|||||||||
26661|Kholo Subgroup|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
26661|Kholo Subgroup|39079|6|Mentioned|p10|||||||||
26661|Kholo Subgroup|39445|6|Mentioned|Table 9|||||||||
26661|Kholo Subgroup|39943|6|Mentioned|Table 12A|||||||||
26661|Kholo Subgroup|40434|6|Mentioned|p25|||||||||
26661|Kholo Subgroup|40623|5|Briefly described|p30|||||||||
26661|Kholo Subgroup|41906|6|Mentioned|p14|||||||||
26661|Kholo Subgroup|42316|6|Mentioned|Fig.2 P6|||||||||
26661|Kholo Subgroup|42336|5|Briefly described|p4|||||||||
26661|Kholo Subgroup|42405|6|Mentioned|Table 3 P.7|||||||||
26661|Kholo Subgroup|42492|5|Briefly described|Table 2 p14|||||||||
26661|Kholo Subgroup|42893|5|Briefly described|Fig.2 p7|||of Ipswich Coal Measures||||||
26661|Kholo Subgroup|43076|5|Briefly described|p8|||of Ipswich Coal Measures||||||
26661|Kholo Subgroup|43922|14|Not recorded|p324,325|||Subgroup of Ipswich Coal Measures.||||||
26661|Kholo Subgroup|44687|6|Mentioned|p221|Late Triassic|Middle Triassic|Of Allen (1959). ?Equivalent to Brisbane Tuff.||||||21-MAR-13
26661|Kholo Subgroup|44705|14|Not recorded|p1,15|||||||||
26661|Kholo Subgroup|44734|14|Not recorded|p6,7|||||||||
26661|Kholo Subgroup|44783|14|Not recorded|p16,18|||||||||
26661|Kholo Subgroup|60281|5|Briefly described|p25|||Piedmont fan conglomerates.  Geological Province: Ipswich Basin.||||||
26661|Kholo Subgroup|64665|5|Briefly described|p57.|Late Triassic|Late Triassic|Ipswich Basin. Generally coal barren.||Lower unit in Ipswich Coal Measures.||Is overlain by Brassall Subgroup.|Alluvial fan deposits, some basalt lavas and air-fall tuffs.|
26661|Kholo Subgroup|67402|5|Briefly described|p165 tbl LPB1, p222, p225|Late Triassic|Late Triassic|Ipswich Basin. ||Ipswich Coal Measures|Includes the Blackwall Breccia, Mount Crosby Formation, Colleges Conglomerate, Hector Tuff and Cribb Conglomerate.|Overlain by the Brassall Subgroup.||
26661|Kholo Subgroup|68679|5|Briefly described|p392-395|Late Triassic|Late Triassic|Ipswich Basin.||Ipswich Coal Measures.|Cribb, Colleges Conglomerates; Hector Tuff; Mount Crosby Formation; Weir, Sugars Basalts; Blackwall Breccia.|Is overlain by Tivoli Formation (Brassall Subgroup).|Has a basal breccia overlain by volcanics: initially mafic then a later felsic phase; above these are siliciclastic sediments and minor tuff horizons, with an uppermost unit dominated by medium- to very coarse-grained sandstone and conglomerate.|
26661|Kholo Subgroup|73306|5|Briefly described|p565-566|Late Triassic|Late Triassic|Ipswich Basin.||||Is overlain by Brassall Subgroup.||
79128|Kidgell Andesite Member|70913|3|Fully described|p49-52, p8 fig 3, p11, p45 fig 6|Middle Permian|Early Permian|Gympie Province. Replaces the informal Hall andesite. Lithologically similar to the Calton Andesite Member. Named for Kidgell Street in Gympie.  Abbreviated to Kidgell Andesite p32, 44, 49, 52, 67, 77, 79. Type locality is given and a reference drill hole is named. Distribution is briefly discussed. Approximately 100m thick. See also App 1 maps.||Dawn Formation||Overliesor within the Hall Clastics Member. Overlain by the Tozer Basalt Member, Mary Basalt.|Hornblende and feldspar-phyric andesite, flow or dome facies and proximal breccia.|18-SEP-17
35228|Kidston Breccia Pipe|23158|5|Briefly described|table4|Proterozoic|Proterozoic|||||||
39146|Kilbeggan Granite|61777|5|Briefly described|p227, p225 Tab. 1||Tournaisian|Age: 319+/-7Ma (SHRIMP U/Pb). Hornblende biotite tonalite.||||||07-FEB-11
39146|Kilbeggan Granite|65388|6|Mentioned|p320|||Impey Granodiorite was previously partly included in this unit by Whitaker & others (1974).||||||
37030|Kilcunda Rhyolite|23251|5|Briefly described|Table 1, p8||Late Triassic|No isotopic dating; relationship to other units indicates a Late Triassic age. See also Kilcunda Rhyolite Member - names used interchangeably. (Table3 p25).||||||21-JUN-06
37030|Kilcunda Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
37030|Kilcunda Rhyolite|44928|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics Group. Rhyolitic ignimbrite.||||||31-MAY-06
37030|Kilcunda Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Felsic pyroclastics; pumice fiamme, biotite, quartz, oligoclase and sanidine crystals in a very fine-grained welded ash and recrystallised glassy groundmass of very fine-grained rhyolitic ash and glass shards; most units densely welded.|
37030|Kilcunda Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
69002|Kildare Granodiorite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Coarse-grained porphyritic (K-feldspar) titanite-bearing biotite granodiorite; coarse grained titanite-bearing hornblende quartz monzonite with numerous microdiorite enclaves and common pink aplite and pegmatite dykes.||||||
69002|Kildare Granodiorite|65388|2|Defined|p323-324, 310, 237, 238,  301, 303|Early Triassic|Late Permian|New unit. Of Tandora Suite. Previously included in Culcraigie Granite. In contact with the Colodon Granodiorite, Wingfield Granite, Tandora Granodiorite and Glencoe Gabbro. Contact relationships masked by soil cover. May have intruded Colodon Granodiorite, Glencoe Gabbro. Age inferred. Mostly coarse-grained, porphyritic titanite-bearing hornblende-biotite monzogranite to granodiorite.  See also p304, 307, 318, 332, 340.||||||
69002|Kildare Granodiorite|68679|5|Briefly described|p419-420|||A circular, ~75 km2 intrusion in the Rawbelle Batholith. Geochemistry plot.||Tandora Suite.||May intrude Colodon Granodiorite and Glencoe Gabbro.|Biotite granodiorite; hornblende quartz monzonite.|
77637|Kilmarnock Suite|43213|5|Briefly described|p117|||The major Suite in the Retreat Supersuite.||Unit in Retreat Supersuite.|Mount Observatory, Llandillo Granites; Kilmarnock, Sunny Park, Central Creek, Bevandale Granodiorites; Iron Hut Quartz Monzonite; Annmore, Stevenson Quartz Monzodiorites; Carney Creek Quartz Diorite.|||
28030|Kimba Gneiss|23420|5|Briefly described|p 144 table 4.4|||In the Newberry Metamorphic Group.||||||
28030|Kimba Gneiss|43596|4|Described|p8, p14, , p20 Tb. 1||Proterozoic|Of Newberry Metamorphic Group. Geological province: Yambo Province, on eastern edge of Coen Inlier. Comprises gneiss, mylonitic granitic gneiss, quartzite, and lesser schist and amphibolite. Detailed lithology included (p20 Tb. 1).||||||07-APR-15
28030|Kimba Gneiss|43665|6|Mentioned|p11||Proterozoic|||||||
28030|Kimba Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|Of Newberry Metamorphic Group.||||||28-FEB-08
28030|Kimba Gneiss|69591|5|Briefly described|p71 Fig.2.69, p73 Tb.2.4|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Scattered exposures on northern JEDDA CREEK and central KALINGA map sheets. Thickness, boundary relationships and relative age are unknown.||Newberry Metamorphic Group.|||Muscovite-biotite-quartz gneiss, feldspar, garnet; sillimanite-muscovite-quartz schist; quartzite, amphibolite, mafic granulite.|
28030|Kimba Gneiss|71792|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Etheridge Province.||Newberry Metamorphic Group||Overlies the Penny Gneiss. Overlain by the Kitja Gneiss.||
22104|King Junction Granite|23420|4|Described|p 152 table 4.8||Early Devonian|Intrudes Burton Lagoon Granite and Aralba Granite||||||
22104|King Junction Granite|43596|4|Described|p34, p28 Tb. 3|||Intrudes the Yambo Metamorphic Group. Strongly porphyritic muscovite-biotite granite and minor garnet-muscovite leucogranite.||||||15-JAN-09
22104|King Junction Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
26665|Kingull Member|23056|6|Mentioned|8 table 1B|||Geol province Surat Basin||||||
26665|Kingull Member|23982|5|Briefly described|p58 Fig.18|||Of Bungil Formation. Geological Province: Surat Basin.||||||
26665|Kingull Member|24092|5|Briefly described|p8 Fig.3|||Of Bungil Formation. Geological Province: Surat Basin.||||||
26665|Kingull Member|30021|6|Mentioned|p87|||||||||
26665|Kingull Member|30022|6|Mentioned|p28|||||||||
26665|Kingull Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26665|Kingull Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
26665|Kingull Member|30696|4|Described|Table 4|||Lower Cretaceous age||||||
26665|Kingull Member|30702|6|Mentioned|p49|||See also P50, 51 & Table 1. Stratigraphic table.||||||
26665|Kingull Member|31116|4|Described|p41|||See also P42||||||
26665|Kingull Member|31208|6|Mentioned|Table 1|||||||||
26665|Kingull Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
26665|Kingull Member|32314|6|Mentioned|Fig. 4|||||||||
26665|Kingull Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
26665|Kingull Member|37995|6|Mentioned|p66|||||||||
26665|Kingull Member|39211|5|Briefly described|p31|||||||||
26665|Kingull Member|39212|4|Described|p39|||Excursion site. See also P18||||||
26665|Kingull Member|40541|4|Described|p111|||||||||
26665|Kingull Member|40666|4|Described|p358|||||||||
26665|Kingull Member|41057|6|Mentioned|p61|||||||||
26665|Kingull Member|41064|6|Mentioned|p60|||||||||
26665|Kingull Member|41681|6|Mentioned|p23|||||||||
26665|Kingull Member|42494|5|Briefly described|Table 1 P24|||||||||
26665|Kingull Member|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
26665|Kingull Member|44021|14|Not recorded|p232(Fig.1)|||||||||
26665|Kingull Member|44023|6|Mentioned|Tb.3,p12|||||||||
26665|Kingull Member|44082|6|Mentioned|Table p34|||Part of Blythesdale Formation. Mention on correlation table of Queensland Cretaceous sediments.||||||
26665|Kingull Member|44377|2|Defined|p1-3,7,10,12,14,map||Neocomian|Freshwater. Member of Blythesdale Formation.||||||
26665|Kingull Member|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965.||||||
26665|Kingull Member|45103|6|Mentioned|p5|||||||||
26665|Kingull Member|45110|4|Described|p111|||See also Table 18. Of Bungil Formation.||||||
26665|Kingull Member|45132|6|Mentioned|Table 2|||||||||
26665|Kingull Member|46791|6|Mentioned|Table 1|||||||||
26665|Kingull Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
26665|Kingull Member|46984|6|Mentioned|Table 1|||||||||
26665|Kingull Member|48919|4|Described|Table 5|||P70||||||
26665|Kingull Member|49010|6|Mentioned|Fig.4|||Surat Basin||||||
26665|Kingull Member|49011|6|Mentioned|Fig.3|||Surat Basin||||||
26665|Kingull Member|64856|5|Briefly described|p98|Early Cretaceous|Early Cretaceous|Of Day (1964). Originally included in Blythesdale Formation, now in Bungil Formation. Inferred to be of Lower Cretaceous age.| | ||||31-JAN-13
26665|Kingull Member|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Bungil Formation.||Is overlain by Nullawurt Sandstone Member.||
26665|Kingull Member|69594|5|Briefly described|p538|||Northern Surat Basin. Previously included by Day (1964) in his Blythesdale Formation.||Bungil Formation.|||Highly calcareous siltstones, cone-in-cone limestones, and some carbonaceous shale interbedded with lithic sandstones.|
26665|Kingull Member|70821|5|Briefly described|p80|||Surat Basin.||Bungil Formation.||Overlies Mooga Sandstone. Is overlain by Nullawurt Sandstone Member.||
26665|Kingull Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||Bungil FZ.||Overlies Mooga Sandstone. Is overlain by Nullawurt Sandstone Member.||
28037|Kingvale Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Granite of the Kintore Supersuite.||||||
28037|Kingvale Granite|43596|4|Described|p31, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Oswald, Saraga and Jedda Schists. Pale grey to buff, coarse, abundantly porphyritic muscovite-biotite granite; euhedral phenocrysts of muscovite and K-feldspar.||||||27-JAN-09
28037|Kingvale Granite|50537|6|Mentioned|p6.1|||||||||
28037|Kingvale Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
27813|Kinrara Basalt|23291|4|Described|p80 Tb. 3.6|Tertiary|Tertiary|Parent: McBride Basalt Group. Age: <40Ka. Geological Province: Georgetown Region.||||||08-JUL-15
27813|Kinrara Basalt|23494|4|Described|p11, p18 Tb. 1|Cenozoic|Cenozoic|Fine-grained, generally vesicular olivine basalt.  Unconformably overlies McBride Basalt.  Max. thickness: <50ft.  Geological Province: McBride Basalt Province.||||||19-NOV-08
27813|Kinrara Basalt|23498|6|Mentioned|p19  table 1|||||||||
27813|Kinrara Basalt|23619|4|Described|p28 table 1||Pleistocene|Olivine basalt. Of the McBride Basalt Group in the McBride Basalt Province.||||||
27813|Kinrara Basalt|31832|6|Mentioned|Table 6|||||||||
27813|Kinrara Basalt|32553|4|Described|p34|||||||||
27813|Kinrara Basalt|33648|6|Mentioned|p23|||Youngest volc. episode in Qld.||||||
27813|Kinrara Basalt|39027|6|Mentioned|Map legend|Recent|Recent|||||||
27813|Kinrara Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
27813|Kinrara Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
27813|Kinrara Basalt|44048|14|Not recorded|Map Legend||Recent|||||||
27813|Kinrara Basalt|44744|14|Not recorded|p106,112|||V.fluid extrusion.||||||
27813|Kinrara Basalt|44796|14|Not recorded|p3,5|||Recent according to Best 1960||||||
27813|Kinrara Basalt|44800|14|Not recorded|p16,22,map|Recent|Pleistocene|(Late Pleistocene-Early Recent)||||||
27813|Kinrara Basalt|45009|2|Defined|p16,91-2,94,96-101,|||fig.1,Pl.13||||||
27813|Kinrara Basalt|45087|5|Briefly described|p167|||Chemical analyses||||||
27813|Kinrara Basalt|45151|5|Briefly described|p23|||||||||
27813|Kinrara Basalt|48903|6|Mentioned|p35|||||||||
27813|Kinrara Basalt|50202|5|Briefly described|Map legend|Quaternary|Quaternary|Of the McBride Basalt Group.  Olivine basalt.  Age: <40Ka.||||||
27813|Kinrara Basalt|68344|5|Briefly described|Map legend.|Quaternary|Quaternary||<40 Ka.|Unit in McBride Basalt Group.|||Olivine basalt.|
27813|Kinrara Basalt|68480|5|Briefly described|Map Legend|Quaternary|Quaternary|McBride Basalt Province. Upper Pleistocene maximum age.|< 0.04 Ma||||Olivine basalt.|
27813|Kinrara Basalt|68481|5|Briefly described|Map Legend|Quaternary|Quaternary|McBride Basalt Province. Upper Pleistocene maximum age.|< 0.04 Ma||||Olivine basalt.|
27813|Kinrara Basalt|68576|5|Briefly described|Q_11: p19-20|Pleistocene|Pleistocene|Youngest unit in the McBride Basalt Province.|70-50 k.y. (K-Ar)|||||
27813|Kinrara Basalt|73115|6|Mentioned|[See comments]|Holocene|Pleistocene|McBride Basalt Province. Represented by a 55 km long lava flow. Age also written as 7 ka. Surface expression is jagged and blocky. Typically associated with rainforests and vine thickets [helpful for remote identification]. Associated with persistent wet areas / springs. Contributes the first reliable [groundwater] input to the Burdekin River. p: 16, 25, 27-29, 32, 39, 43, 48, 53, 59, 61, 63, 65, 68, 132.|7-20 ka|||||
27086|Kintore Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
27086|Kintore Granite|22781|4|Described|p33|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
27086|Kintore Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Coen Metamorphc Group, Lankelly Granite and Morehead Granite. Age: 407 Ma||||||
27086|Kintore Granite|23431|5|Briefly described|p535|||Iron Range Province.||||||
27086|Kintore Granite|42610|1|Redefined|p6|Early Devonian|Late Silurian|Redefinition of the "Kintore Adamellite". Age 406+/-7Ma.||||||
27086|Kintore Granite|43596|4|Described|p35, p26 Tb. 2, p27 Tb. 3|||Of Ebagoola Suite (Kintore Supersuite). Together with Morehead and Imooya Granites forms core of Cape York Peninsula Batholith. Intrudes Dinah, Strathburn+Astrea Fms,Gorge Qtz'ite.Outcrops as distinctive unweathered boulders. detailed lithology presented.||||||15-JAN-09
27086|Kintore Granite|43738|6|Mentioned|p5|||||||||
27086|Kintore Granite|43741|3|Fully described|p7,21|Devonian|Silurian|Ages(U-Pb): 406+/-7 Ma, 409+/-6 Ma||||||
27086|Kintore Granite|69592|5|Briefly described|p282, p288 Fig.4.84|||Cape York Peninsula Batholith. REE plot.|408 +/- 10 Ma; 405 +/- 9  Ma (SHRIMP U-Pb zircon).|Kintore Supersuite.|||S-type.|
27086|Kintore Granite|70207|5|Briefly described|p125-126|Early Devonian|Late Silurian||~406 Ma.|||Intrudes Sefton Metamorphics.||
27086|Kintore Granite|71031|6|Mentioned|p15, p20||||408 +/- 10 Ma, 405 +/- 9 Ma (Black et al 1992a,b)|||||
27086|Kintore Granite|71592|5|Briefly described|Appendix A.|||Palma Igneous Province.|408+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
27086|Kintore Granite|71792|5|Briefly described|p26, p31|||Rocks formerly mapped as this unit have since been reassigned to the Buthen Buthen Granite. ||||||
27086|Kintore Granite|71849|4|Described|p8, p14, p36, p61, p67-70, p102, p104|Devonian|Devonian|See also p111, p149, p152, p154-158, p162, p176, p195. Previously Kintore Adamellite (Trail et al.,1969 and others). Small intrusions and scattered outcrops over an extensive area. Main component of the Supersuite. Geophysics briefly described; lithology and geochemistry described and contrasted with Lankelly Granite.|406 +/- 7 Ma SHRIMP: Black et al. (1992).|Ebagoola Suite.||Adjacent to (probably intrudes) Lankelly Granite.|Pale grey, medium-grained, even-grained to slightly porphyritic muscovite-biotite monzogranite. Moderately deformed. Mainly high-K calc-alkaline S-type.|
27086|Kintore Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Pale grey to cream or brown, even-grained to slightly porphyritic biotite-muscovite granite; locally garnet-bearing; K-feldspar phenocrysts typically 2-4cm long; moderately deformed.|
27086|Kintore Granite|72983|6|Mentioned|p5, p56, p104, p106|Early Devonian|Early Devonian|New ages led to a mapped outcrop of this unit being reassigned to the Choc-a-block Orthogneiss. Interleaved with unnamed hypabyssal Carboniferous intrusives in the Mangkuma Land Trust area.||||Intrudes Coen Metamorphic Group including[?] Yarraden Schist.|Muscovite-rich S-type granite.|
27086|Kintore Granite|73083|6|Mentioned|p59|||||||||
27086|Kintore Granite|73387|6|Mentioned|p1, p37|Early Devonian|Early Devonian|Magmatic crystallisation ages of 405 +/- 9 Ma, 406 +/- 7 Ma, and 408 +/- 10 Ma from Black et al. (1992). Ages are indistinguishable from metamorphic ages in the Coen Metamorphic Group.|405 +/- 9 Ma, 406 +/- 7 Ma, 408 +/ 10 Ma|||||
28165|Kirk River beds|22847|4|Described|p7|||May in part be equivalent to the Puddler Creek Formation, Seventy Mile Range Group.||||||
28165|Kirk River beds|23422|5|Briefly described|p171, p206 Table 6.3|Middle Ordovician|Cambrian|Regarded as equivalent to Puddler Creek Formation of Seventy Mile Range Group (p71). Not part of Seventy Mile Range Group, as suggested in Table.||||||
28165|Kirk River beds|23504|5|Briefly described|Map Legend|Ordovician|Cambrian|NOT of Seventy Mile Range Group. See 00/30577 and 98/28898||||||
28165|Kirk River beds|23509|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
28165|Kirk River beds|23893|5|Briefly described|p12|Early Devonian|Late Cambrian|Geological Province: Thalanga Province.||||||
28165|Kirk River beds|24612|6|Mentioned|p9 Fig.2|||Mentioned in terms of Kirk River beds equivalents only.||||||20-DEC-04
28165|Kirk River beds|24613|5|Briefly described|p6 Fig. 3|Early Devonian|Precambrian|Geological province: Burdekin Basin.||||||07-FEB-11
28165|Kirk River beds|36472|6|Mentioned|Map legend|Ordovician|Cambrian|Ordovician to Cambrian||||||
28165|Kirk River beds|42245|5|Briefly described|p32|||||||||
28165|Kirk River beds|42295|6|Mentioned|Fig.2 P5|||||||||
28165|Kirk River beds|43093|5|Briefly described|p11|||see also Fig.1.||||||
28165|Kirk River beds|43935|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
28165|Kirk River beds|43936|5|Briefly described|Map Legend|Ordovician|Cambrian|Shown as part of the Seventy Mile Range Group, but this seems to be a drafting error. See  'Geology of the Ravenswood Batholith' 1997 (00/30577)||||||
28165|Kirk River beds|45151|6|Mentioned|p4|||||||||
28165|Kirk River beds|62074|5|Briefly described|p1|Early Ordovician|Late Cambrian|Sedimentary rocks and felsic to intemediate volcanic rocks. Assigned to the Thalanga Province; forms a roughly E-W belt across S margin of Lolworth-Ravenswood Block.||||||
28165|Kirk River beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Ordovician|Cambrian|Mount Windsor Subprovince. This unit, as well as Seventy Mile Range Group and Les Jumelles beds, are all mapped under the symbol, -COs.||||||
28165|Kirk River beds|68731|5|Briefly described|p136|Early Ordovician|Late Cambrian|Charters Towers Province. Lies within the Ravenswood Batholith east-northeast of Charters Towers. A possible outlier of the Puddler Creek Formation.||||Unconformably overlain by the Ewan Formation.||
28165|Kirk River beds|68900|6|Mentioned|p4|Early Ordovician|Cambrian|Drummond Basin.||Seventy Mile Range Group||||
25125|Kirklea Granite|22847|3|Fully described|p 41|||||||||
25125|Kirklea Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
25125|Kirklea Granite|23504|5|Briefly described|Map Legend||Ordovician|||||||
25125|Kirklea Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 100.  Assumed to be I-Type.||||||
25125|Kirklea Granite|24424|5|Briefly described|p526|Ordovician|Ordovician|Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
25125|Kirklea Granite|30148|2|Defined|p17|Early Devonian|Late Silurian|Middle Ordovician & Upper Silurian or Lower Devonian.||||||
25125|Kirklea Granite|30149|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician and Upper Silurian or?Lower Devonian||||||
25125|Kirklea Granite|30151|4|Described|Table 1|||Ravenswood Granodiorite Complex.||||||
25125|Kirklea Granite|31813|6|Mentioned|Table 2|||||||||
25125|Kirklea Granite|34409|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician, Upper Silurian, Lower Devonian||||||
25125|Kirklea Granite|39686|6|Mentioned|p75|||||||||
25125|Kirklea Granite|41668|6|Mentioned|p12|||||||||
25125|Kirklea Granite|42245|6|Mentioned|p36|||||||||
25125|Kirklea Granite|43093|4|Described|Appendix 1|||Rb-Sr age of 470+/-30Ma.||||||
25125|Kirklea Granite|43259|4|Described|Appendix 1,p22.||Ordovician|||||||
25125|Kirklea Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
25125|Kirklea Granite|43936|5|Briefly described|Map Legend||Ordovician|||||||
25125|Kirklea Granite|48914|2|Defined|p82|Early Devonian|Late Silurian|U.Sil. - L.Dev.||||||
25125|Kirklea Granite|50552|5|Briefly described|p1049 Fig.3|Middle Ordovician|Early Ordovician|In Lolworth-Ravenswood Terrane.||||||
25125|Kirklea Granite|62075|6|Mentioned|p11 Fig.4|Middle Ordovician|Early Ordovician|Hadleigh Castle area, Charters Towers goldfields. Appears as Kirklea granite.||||||
34689|Kirkton Tonalite|22847|3|Fully described|p 54|||||||||
34689|Kirkton Tonalite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
34689|Kirkton Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 192. I-Type.||||||
34689|Kirkton Tonalite|43936|5|Briefly described|Map legend|Devonian|Silurian|||||||
34689|Kirkton Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Kirkton ton.||||||
23701|Kirkwood Monzogranite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
23701|Kirkwood Monzogranite|22781|4|Described|p29|Paleozoic|Paleozoic|Flyspeck  Supersuite||||||07-NOV-08
23701|Kirkwood Monzogranite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intruded by Barwon Granite and Ebagoola Granite||||||
23701|Kirkwood Monzogranite|42610|2|Defined|p29|Early Devonian|Early Devonian|Age ass. sim. Two Rail Monzogran. Prev.incl. in "Flyspeck Gran." & "Kintore Adamell." B135.||||||
23701|Kirkwood Monzogranite|43738|6|Mentioned|Fig.12,p38|||||||||
23701|Kirkwood Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
23701|Kirkwood Monzogranite|71849|6|Mentioned|p120|||Significance of allanite-epidote association discussed.||Flyspeck Supersuite.||||
23701|Kirkwood Monzogranite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Flyspeck Supersuite.|||Pale grey, sparsely porphyritic, biotite monzogranite with K-feldspar phenocrysts typically 2cm x 1cm.|
28116|Kitchen Creek Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Kungaree Volcanic Subgroup. Thickness: 180-200m. Geological Province: Georgetown Region.||||||02-JUL-15
28116|Kitchen Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V21. Assumed to be I-Type.||||||
28116|Kitchen Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
28116|Kitchen Creek Rhyolite|40542|6|Mentioned|p97|||||||||
28116|Kitchen Creek Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Kungaree Volcanic Subgroup.||||||
28116|Kitchen Creek Rhyolite|43740|4|Described|p9|||||||||
28116|Kitchen Creek Rhyolite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Kungaree Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
28116|Kitchen Creek Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Kungaree Volcanic Subgroup.|||Grey to brown or purple crystal-poor to moderately crystal-rich rhyolitic ignimbrite, locally containing sparse chlorite; kaolinised rhyolite is mapped separately.|
28116|Kitchen Creek Rhyolite|68576|5|Briefly described|Q_11: p22 Fig.20, p23|Carboniferous|Carboniferous|Routh Creek. A single rhyolite sheet up to 180m thick.||Kungaree Volcanic Subgroup.|||Purplish brown, moderately crystal-rich rhyolitic ignimbrite with a well-developed eutaxitic fabric defined by flattened pumice fragments or fiamme; crystal fragments include quartz and feldspar; some chlorite aggregates locally.|
29311|Kitchener Granite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes Martin Creek Microgranite and Sheba Granite; intruded by Ootann Granite. Geological Province: Georgetown Region.||||||08-JUL-15
29311|Kitchener Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
29311|Kitchener Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29311|Kitchener Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 322. I-Type.||||||
29311|Kitchener Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29311|Kitchener Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type. Lithology included.||||||01-JUL-15
29311|Kitchener Granite|43087|2|Defined|p31|Late Carboniferous||||||||
29311|Kitchener Granite|60425|4|Described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. Pink to cream, med.-to coarse-gr., even-gr., to slightly porphyritic granite; rare hornblende + mafic enclaves; commonly moderately to extensively altered (greisenised); + deposits of molybdenum - more lith.detail||||||07-FEB-11
29311|Kitchener Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium- to fine-grained, porphyritic (allanite-hornblende-)biotite monzogranite; extensively altered.|
29758|Kitja Gneiss|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Newberry Metamorphic Group||||||12-JAN-05
29758|Kitja Gneiss|22781|4|Described|p11|Proterozoic|Proterozoic|Newberry Metamorphic Group||||||
29758|Kitja Gneiss|23420|5|Briefly described|p 144 table 4.4|Calymmian|Calymmian|In the Newberry Metamorphic Group. Age:1564 +/- 12Ma||||||
29758|Kitja Gneiss|43596|5|Briefly described|p14, p20 Tb. 1|||Of Newberry Metamorphic Group. Contains massive quartzite, muscovite quartzite and schist, sillimanite-mica-feldspar-quartz gneiss and local bodies of mafic granulite.||||||27-JAN-09
29758|Kitja Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|Newberry Metamorphic Group||||||24-JAN-05
29758|Kitja Gneiss|69591|5|Briefly described|p73 Tb.2.4|Paleoproterozoic|Paleoproterozoic|Mostly concealed band 100km long by 15km wide, from Mount Newberry south to the Hann River. Thickness, boundary relationships and relative age are unknown. Age is for crystallisation of the igneous precursor.|1564 +/- 12 Ma.|Newberry Metamorphic Group.|||Quartzite, minor muscovite, haematite; (sillimanite-)muscovite-biotite-feldspar-quartz gneiss.|
29758|Kitja Gneiss|71792|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|1564 Ma (Magmatic crystallisation)|Newberry Metamorphic Group||Overlies the Kimba Gneiss.||
29758|Kitja Gneiss|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Newberry Metamorphic Group.|||Thick layers of coarse massive quartzite; minor muscovite, hematite; some mafic plagioclase-orthopyroxene-hornblende granulite in deeply-weathered garnet-biotite-sillimanite-kyanite-plagioclase-K-feldspar-quartz gneiss.|
36211|Kitty O'Shea Suite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
36211|Kitty O'Shea Suite|24613|5|Briefly described|p114|||See also the informal Kitty O'Shea suite and "Kitty O'Shea suite", also on p64 and p113.||||||07-FEB-11
36211|Kitty O'Shea Suite|68419|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Kennedy Province. Minimum age shown as Early Permian.|||||Microdiorite, dolerite, gabbro, and intrusive andesite and basalt.|
36211|Kitty O'Shea Suite|68420|5|Briefly described|Map Legend|Early Permian|Carboniferous|Of the Kennedy Province.|||||Microdiorite, dolerite, gabbro, and intrusive andesite and basalt.|
74109|Kitty Plain Microgranite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|In part is part of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
74109|Kitty Plain Microgranite|67323|5|Briefly described|GIS attrib tbl, p12|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Exhibits NW trending linear fabric.||Sybella Suite|||Slightly porphyritic, fine to medium-grained alkali granite to granodiorite; locally abundant metasedimentary and mafic xenoliths, as well as mafic pillows/enclaves.|
74109|Kitty Plain Microgranite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Slightly porphyritic, fine- to medium-grained alkali granite to granodiorite; locally abundant metasedimentary and mafic xenoliths, as well as mafic pillows/enclaves.|
36274|Knob Camp Granodiorite|23291|4|Described|p46, p97 Tb. 3.11|Early Permian|Early Permian|Intrudes rocks of the Scardons Volcanics Group aged 290 +/- 3 Ma. Parent: Brodies Camp Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
36274|Knob Camp Granodiorite|23510|5|Briefly described|Map Legend||Early Permian|of Brodies Camp Supersuite.||||||
36274|Knob Camp Granodiorite|68405|5|Briefly described|Map Legend|Permian|Permian|Kennedy Province? Early Permian ?||Of the Brodies Camp Supersuite.|||Porphyritic biotite-hornblende granodiorite.|
36274|Knob Camp Granodiorite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Brodies Camp Supersuite.|||A-type.|
78845|Kogan seam package|65096|6|Mentioned|p372|Middle Jurassic|Middle Jurassic|[informal 'sequence stratigraphy' unit] Top 'seam package' of Juandah Coal Measures. See also fig.2, p370. Difficult to distinguish from Wambo and MacAlister seam packages on basis of wireline logs.||Said to be of the Juandah Coal Measures sequence.||||
22121|Kokojelandji Schist|23420|5|Briefly described|p 144 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
22121|Kokojelandji Schist|43285|5|Briefly described|Map Legend|||age Middle Proterozoic.||||||
22121|Kokojelandji Schist|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
22121|Kokojelandji Schist|43596|5|Briefly described|p13, p20 Tb. 1||Proterozoic|Of Yambo Metamorphic Group. Consists predominantly of sillimanite-quartz-sericite schist, with rare garnet porphyroblasts and zircon; the sericite pseudomorphs sillimanite. Commonly interlayered with schistose fine-grained, sillimanite-sericite quartzite.||||||27-JAN-09
22121|Kokojelandji Schist|43625|5|Briefly described|p15,Table 1||Mesoproterozoic|Age: pre-1590 Ma||||||
22121|Kokojelandji Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Yambo Metamorphic Group||||||24-JAN-05
22121|Kokojelandji Schist|60357|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Yambo Subprovince. Of the Yambo Metamorphic Group.||||||07-NOV-08
22121|Kokojelandji Schist|60358|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Yambo Metamorphic Group. Sillimanite-muscovite schist, quartzite. Geological Province: Yambo Subprovince.||||||07-NOV-08
22121|Kokojelandji Schist|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier.||Yambo Metamorphic Group.|||Sillimanite-sericite-quartz(+/- garnet) schist; interlayered schistose, fine-grained sillimanite-sericite quartzite.|
28018|Kokomini Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite.||||||
28018|Kokomini Granite|23496|5|Briefly described|Table 2, p40|Devonian|Silurian|of Aralba Suite, Kintore Supersuite.||||||
28018|Kokomini Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Aralba Suite.||||||
28018|Kokomini Granite|43596|4|Described|p31, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Pombete and Arkara Gneiss, and Aralba Granite(?). pale grey, med-gr., even-gr. to slightly porphyritic garnet-biotite-muscovite granite with scattered pegmatite zones, sparse K-feldspar+muscovite phenocrysts.||||||07-APR-15
28018|Kokomini Granite|69592|6|Mentioned|p282, p287 Fig.4.81|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
25976|Kolbar Formation|24382|5|Briefly described|Map legend|Permian|Permian|Parent: Gympie Group.||||||14-AUG-08
25976|Kolbar Formation|41736|2|Defined|p118|Early Permian||Reserved as Kolbar.||||||14-AUG-08
25976|Kolbar Formation|42054|6|Mentioned|p272|||||||||
25976|Kolbar Formation|43017|5|Briefly described|Fig.3,p375|||||||||
25976|Kolbar Formation|63821|4|Described|p17, p18, p40|Early Permian|Early Permian|Of the Gympie Group. Geological Province: Gympie Province. Consists of calcareous and non-calcareous siltstone, arenite and mudstone, and minor acid pyroclastic rocks. Probably deposited in a marine enviornment from a volcanic source.||||||07-FEB-11
25976|Kolbar Formation|68679|5|Briefly described|p370|Sakmarian|Sakmarian|Southern Gympie Province. Crops out from Running Creek to 5km N of Gigoomgan. 350m thick. Contains Sakmarian marine fossils.||||Correlated with Rammutt Formation.|Calcareous and non-calcareous siltstone, sandstone and mudstone and minor felsic volcaniclastics.|
25976|Kolbar Formation|73303|4|Described|p61 Fig.2, p62-64, p66 Fig.6, p67-68|Kungurian|Cisuralian|New England Orogen. Gympie Terrane, northern. Lowermost unit in northern Gympie Terrane, Mant Basalt included as a member in the formation (p64). Thick calcareous mudstones in upper part contain Zoophycus, Phycosiphon and Spirophycus ichnofossils. Brachiopod fauna corresponds to 'Echinalosia warwicki' zone (287-285 Ma), uppermost exposures correspond to the 'upper Echinolosia preovalis' brachiopod range-zone and constrain early Permian age. Brachiopod assemblages correlative with Dawn Formation and Rammutt Formation. Deep marine depositional environment with volcanic sediment source indicated by volcaniclastic turbidites interbedded with dominantly hemipelagic mudstone. See also p69 Fig.10.|287-277 Ma||Mant Basalt|Underlies Gigoomgan Limestone.|Dominated by massive olive-green silicified mudstone, interbedded with volcaniclastic and/or subaqueous volcanic rocks. Includes basaltic unit. Thick horizons of calcareous mudstone in upper part with ichnofossils.|
23703|Koobaba Granite|23423|6|Mentioned|p247|||Whypalla Supersuite||||||
23703|Koobaba Granite|23430|5|Briefly described|p499|||Daintree Subprovince. Kennedy Province.||||||
23703|Koobaba Granite|42304|3|Fully described|p27|||Reserved April 1988 by R.J. Bultitude||||||
23703|Koobaba Granite|42968|5|Briefly described|Fig.1,p91|||||||||
23703|Koobaba Granite|43625|6|Mentioned|p60,124,Appendix 6|||||||||
23703|Koobaba Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
23703|Koobaba Granite|60425|4|Described|p81, p276-7 Appdx. |Early Permian|Early Permian|Of Whypalla Suite (Whypalla Supersuite). S-type. Fine- to coarse-gr., mod'ly to highly porphyritic tourmaline-garnet-muscovite-biotite granite.Comprises several small scattered plutons. Extensively deformed/miarolitic cavities present. More lith.included||||||07-FEB-11
23703|Koobaba Granite|66852|5|Briefly described|pp937-938, p941.|||Shows evidence of syntectonic emplacement. Southern elongate plutons show curved geometry from meridional to WNW-ESE, affected by the Desailly Structure; northern plutons do not.||Unit in Whypalla Supersuite.||||
23703|Koobaba Granite|69592|5|Briefly described|p248, p249 Fig.4.34|Permian|Permian|Central Palmer-Barron Subprovince.||||Intrudes Hodgkinson Formation.||
23703|Koobaba Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Suite.||||
69501|Koogangoona Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, even-grained to rarely porphyritic biotite granite; commonly highly altered.|
69501|Koogangoona Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, even-grained to rarely porphyritic biotite granite; commonly highly altered.|
69501|Koogangoona Granite|69593|5|Briefly described|p486||||318.8 +/- 3.3 Ma.|O'Briens Creek Supersuite.||||
78932|Kooingal Granodiorite Complex|65388|3|Fully described|p263-264, p236 Fig. 81, p237, 238|Late Carboniferous|Late Carboniferous|Replaces Kooingal Granite Complex. Probably intrudes surrounding Torsdale Volcanics. Rb-Sr isochron age: 311+/-29 Ma Webb & McDougall (1968). Overlain disconformably by the Mount Bulgi Conglomerate Member of Camboon Volcanics. Two mingled granitoid types, well exposed. Main type is white to grey, medium-grained, biotite-hornblende granodiorite containing enclaves of grey, fine to medium-grained, porphyritic diorite.||||||
78932|Kooingal Granodiorite Complex|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. The age comment is "Plots along a 311 +/- 29 Ma composite Rb-Sr isochron".|311 +/- 29 Ma (Webb abd McDougall, 1968).|||Intrudes Torsdale Volcanics. Is overlain disconformably by Mount Bulgi Conglomerate Member (Camboon Volcanics).|White to grey, medium-grained hornblende-biotite granodiorite mingled with porphyritic grey diorite that appears to form xenoliths.|
36682|Koolmoon Volcanic Group|23616|5|Briefly described|Table 3 p44|||||||||
36682|Koolmoon Volcanic Group|66529|6|Mentioned|p60|Late Carboniferous|Late Carboniferous||||Includes Glen Gordon Volcanics.|||
36682|Koolmoon Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Elimeek and Wallaman Falls Volcanics; Janet Ranges, Silent Creek and Torres Strait Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
36682|Koolmoon Volcanic Group|69030|6|Mentioned|p6|Permian|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.||||||
36682|Koolmoon Volcanic Group|69593|6|Mentioned|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
70414|Koonanella Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pink, fine to medium-grained, equigranular biotite granite; locally mineralised (chalcopyrite and pyrite).|
70414|Koonanella Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, fine- to medium-grained, equigranular biotite granite; local chalcopyrite and pyrite.|
70414|Koonanella Granite|73450|6|Mentioned|p16|||||||||
22131|Koorboora Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
22131|Koorboora Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 317. I-Type.||||||
22131|Koorboora Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22131|Koorboora Granite|43087|6|Mentioned|p31|||||||||
22131|Koorboora Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22131|Koorboora Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|Late? Carboniferous in age.||||||
22131|Koorboora Granite|60425|5|Briefly described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pink, coarse-grained biotite granite.||||||07-FEB-11
22131|Koorboora Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pale pink, medium-grained, moderately porphyritic, leucocratic biotite monzogranite.|
32145|Kooyong Gabbro|23037|5|Briefly described|p88,9,90|Permian|Silesian|||||||
32145|Kooyong Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgky].  Dark grey, medium-grained gabbro.||||||
32145|Kooyong Gabbro|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
32145|Kooyong Gabbro|65388|3|Fully described|p324-325, p237, 238,  301, 325|Early Triassic|Late Permian|Intrudes Torsdale Volcanics. Relationship to the Wingfield Granite is unclear. Age inferred.  Hornblende gabbro or possibly diorite.||||||
32145|Kooyong Gabbro|68679|5|Briefly described|p417, p419|||A circular, ~4km diameter pluton in the northern part of the Rawbelle Batholith.||||Intrudes Torsdale Volcanics.|Gabbro.|
28036|Kopo Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group||||||
28036|Kopo Granite|43596|4|Described|p31,  p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite).  Intrudes Saraga Schist. Pale grey to buff, coarse, abundantly porphyritic muscovite-biotite granite; euhedral phenocrysts of muscovite and K-feldspar.||||||27-JAN-09
28036|Kopo Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
24344|Korenan Oil Shale Member|40247|4|Described|p211|||||||||
24344|Korenan Oil Shale Member|40954|6|Mentioned|p133|||||||||
24344|Korenan Oil Shale Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably overlain by the Makowata Oil Shale Member. Conformably underlain by the Wheatley Oil Shale Member.|Dark brown to dusky yellowish-brown very thinly laminated oil shale, including minor sideritic argillite with traces of bioturbation.|
24344|Korenan Oil Shale Member|68421|5|Briefly described|Map Legend|Eocene|Eocene|Lowmead Graben.||Of the Lowmead Formation.||Conformably underlain by the Wheatley Oil Shale Member.|Dark brown to dusky yellowish-brown very thinly laminated oil shale, including minor sideritic argillite beds with traces of bioturbation.|
24344|Korenan Oil Shale Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. 94.3 - 156.9m thick, averaging 123.7m.||Lowmead Formation.||Overlies Wheatley Oil Shale Member. Is overlain by Makowata Oil Shale Member.|Oil shale averaging <50 LTOM.|
35120|Koumala Granite|23042|5|Briefly described|p44,86,7, Fig 2|Cretaceous|Jurassic|Intrudes the Carmila beds.||||||
35120|Koumala Granite|60473|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of the Urannah Batholith.  Pale pink to pink, medium to even grained, leococratic biotite monzogranite to syenogranite.||||||17-SEP-04
35120|Koumala Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35120|Koumala Granite|65388|3|Fully described|p407-408, p403 Fig. 135|Early Cretaceous|Early Cretaceous|Intrudes and has hornfelsed rocks assigned to Mountain View Volcanics. Tentative age given. Pale to medium pink, fine to medium-grained, uneven-grained to slightly porphyritic, leucocratic biotite monzogranite at type locality.||||||
35120|Koumala Granite|69594|5|Briefly described|p570, p571 Fig.7.47|Early Cretaceous|Early Cretaceous|Geochemistry plot and discussion.||||||
27453|Kungaree Volcanic Subgroup|23291|4|Described|p40, p95 Tb. 3.10|Permian|Carboniferous|Parent: Newcastle Range Volcanic Group. Geological Province: Georgetown Region.||||||28-MAY-15
27453|Kungaree Volcanic Subgroup|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Newcastle Range Volcanic Group.||||||
27453|Kungaree Volcanic Subgroup|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27453|Kungaree Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
27453|Kungaree Volcanic Subgroup|43740|5|Briefly described|p8|||||||||
27453|Kungaree Volcanic Subgroup|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group. Comprises: Shamrock Rhyolite, Routh Dacite, Corkscrew Rhyolite, Kitchen Creek Rhyolite.||||||28-MAY-15
27453|Kungaree Volcanic Subgroup|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Newcastle Range Volcanic Group.|Includes Shamrock, Corkscrew and Kitchen Range Rhyolites and Routh Dacite.|||
27453|Kungaree Volcanic Subgroup|68576|5|Briefly described|Q_11: p21, p23|Carboniferous|Carboniferous|Forms the Kungaree Trough.||Newcastle Range Volcanic Group.|Kitchen Creek Rhyolite.|||
27453|Kungaree Volcanic Subgroup|70207|5|Briefly described|p14, p81-83, p85|Permian|Permian|Georgetown region.|c.290 Ma.|Newcastle Range Volcanic Group.|Routh Dacite, Corkscrew Rhyolite.||A-type.|
33964|Kunwarara magnesite|22543|6|Mentioned|p67|Cenozoic|Cenozoic|||||||04-MAR-16
76887|Kurbayia Metamorphic Complex|67323|5|Briefly described|GIS attrib tbl, p14, p23, p39-40, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Kalkadoon-Leichhardt Domain, central Mount Isa Block.|||||Dark grey migmatitic meta-pelitic gneiss, tonalitic to granitic gneiss, and subordinate mafic gneiss; rare meta-dacite and pelitic schist|
76887|Kurbayia Metamorphic Complex|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
76887|Kurbayia Metamorphic Complex|68575|6|Mentioned|p118|||Part of the basement in Duchess and Dajarra 1:100 000 sheet areas.|||Tewinga Gneiss.|||
76887|Kurbayia Metamorphic Complex|69591|5|Briefly described|p29, p31, p58|Paleoproterozoic|Paleoproterozoic|One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma). Has strong gneissic to migmatitic foliation.|1857 +/- 5 Ma (Geoscience Australia unpub. data).||||Dioritic to granitic gneiss (commonly with mafic metasedimentary inclusions), migmatitic porphyroclastic granitic gneiss, finely porphyritic felsic gneiss and minor pelitic schist.|
76887|Kurbayia Metamorphic Complex|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1857+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
76887|Kurbayia Metamorphic Complex|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Post-Barramundi Orogeny ~1870 Ma. Two informal subdivisions shown.||||Shown as older than Kalkadoon Granodiorite.  Shown as age equivalent to Leichhardt Volcanics.|Dark grey migmatitic metapelitic gneiss, tonalitic to granitic gneiss, and subordinate mafic gneiss; rare metadacite and schist. Pale grey, medium to coarse-grained, equigranular, strongly foliated granitic gneiss. Rare mafic gneiss and migmatite.|
76887|Kurbayia Metamorphic Complex|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Post-Barramundi Orogeny ~1870 Ma. Two informal subdivisions shown.||||Shown as older than Kalkadoon Granodiorite.  Shown as age equivalent to Leichhardt Volcanics.|Dark grey migmatitic metapelitic gneiss, tonalitic to granitic gneiss, and subordinate mafic gneiss; rare metadacite and schist. Pale grey, medium to coarse-grained, equigranular, strongly foliated granitic gneiss. Rare mafic gneiss and migmatite.|
76887|Kurbayia Metamorphic Complex|72889|6|Mentioned|p6 Fig.i, p14.|||Located in the southern part of the Kalkadoon-Leichhardt Domain.|c. 1870-1840 Ma.|||||
76887|Kurbayia Metamorphic Complex|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
76887|Kurbayia Metamorphic Complex|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Kalkadoon-Leichhardt Domain. Crystallisation of intrusion age of 1857+/-5 Ma.|||||Metamorphics.|
29289|Kurungle Volcanics|31984|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
29289|Kurungle Volcanics|32553|4|Described|p44|||||||||
29289|Kurungle Volcanics|32556|4|Described|Table 3|||L.Perm.||||||
29289|Kurungle Volcanics|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
29289|Kurungle Volcanics|37613|5|Briefly described|p249|||See also Fig.3||||||
29289|Kurungle Volcanics|45151|6|Mentioned|Table 7|||||||||
29289|Kurungle Volcanics|48922|3|Fully described|p43|||||||||
29289|Kurungle Volcanics|65706|5|Briefly described|p84, p145|Early Cretaceous||Also referred to as the Kurungle Volcanic suite. Includes a geochemically anomalous (for Cu-Mo) alteration-breccia zone and a pyroclastic sequence.||||||
29289|Kurungle Volcanics|73450|6|Mentioned|p43|early Permian|early Permian|||||Intruded by Mount Abbot Igneous Complex.||
25139|Kurwongbah beds|22845|6|Mentioned|p12|Early Carboniferous|Late Devonian|Correlates with Gobongo Metamorphics.||||||
25139|Kurwongbah beds|23251|6|Mentioned|p3|||Was previously included in the Gympie Group by Day & others (1978). Gympie Group||||||
25139|Kurwongbah beds|23799|6|Mentioned|p21|||||||||
25139|Kurwongbah beds|24418|5|Briefly described|p5, Map 1|Carboniferous|Carboniferous|Consists of phyllite, slate containing relatively abundant intercalated lenses of basic metavolcanics, and minor chert bands. Strongly deformed unit. Age: Carboniferous?||||||30-JUN-06
25139|Kurwongbah beds|38805|6|Mentioned|Fig.1|||||||||
25139|Kurwongbah beds|39079|5|Briefly described|p6|||||||||
25139|Kurwongbah beds|40051|6|Mentioned|p5|||||||||
25139|Kurwongbah beds|40623|5|Briefly described|p53|||||||||
25139|Kurwongbah beds|41917|6|Mentioned|p521|||||||||
25139|Kurwongbah beds|42619|6|Mentioned|p29|||||||||
25139|Kurwongbah beds|42694|5|Briefly described|map legend|Carboniferous|Pre-Carboniferous|||||||
25139|Kurwongbah beds|42970|5|Briefly described|p121|||||||||
25139|Kurwongbah beds|43006|5|Briefly described|Table 1,p239|||||||||
25139|Kurwongbah beds|43076|5|Briefly described|p5|||||||||
25139|Kurwongbah beds|43092|4|Described|p13|||see also map enclosure||||||
25139|Kurwongbah beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor and Booloumba beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
25139|Kurwongbah beds|68679|5|Briefly described|p321, p324, p326-328, p332, p334, p369|Carboniferous||Murphy et al. (1976); Murray and Whitaker (1982). Northern New England Orogen. Occurs as a ~2km thick coherent tectonostratigraphic unit, from Petrie to Wamuran. Forms a series of fault slices within a 1-3 km thick imbricate fault zone adjacent to Rocksberg Greenstone, and small slivers within the latter unit. Detachment zone and lower plate accretionary assemblages.||||Tectonically interleaved with Rocksberg Greenstone. Is correlated with Gobongo Metamorphics.|Thinly laminated feldspathic psammopelite with numerous thin quartz-rich layers; abundant mylonitic structures; fine-grained, foliated greenschist layers interlaminated with siliceous phyllite layers.|
39147|Kyle Mohr Igneous Complex|24615|5|Briefly described|CD|Permian|Permian|[Pgkm/d].  Grey to dark grey, medium-grained biotite-hornblende diorite, hornblende diorite and quartz diorite, and altered locally hypersthene-bearing ophitic biotite-augite-hornblende gabbro.||||||
39147|Kyle Mohr Igneous Complex|50317|5|Briefly described|Map Legend|Permian|Permian|||||||
39147|Kyle Mohr Igneous Complex|68008|3|Fully described|p2, p123, p131, p153-156, p321-324, p326|Permian|Permian|See also p329, p483-484, p491, p528. A pluton mapped and described as the Kyle Mohr Granodiorite by Kirkegaard et al. (1970). Comprises an 8.5 x 4 km granodiorite core with a dioritic to gabbroic ring up to 2km wide. Named after the Kyle Mohr holding in the SW. No type area; typical outcrops occur along the headwaters of Oaky Creek. Forms an elevated area with radial streams. Geophysical expression described. Probably co-magmatic with mid-Permian Rookwood Volcanics: their geochemistry compared in detail. Veins parallel and adjacent to the SE margin host the Dee Cu mine. U-Pb zircon age of felsic phase.|270.6 +/- 3.7 Ma (Fanning, 2012).|||Intrudes Balaclava Formation and Youlambie Conglomerate.|Bimodal granite-gabbro intrusion. Leucocratic biotite-hornblende granodiorite (locally granite) core; plagioclase always the dominant mineral. Outer ring of mafic-rich, altered gabbro with local granite dykes. Massive and apparently undeformed.|
39147|Kyle Mohr Igneous Complex|68679|5|Briefly described|p337, p423-425, p470|||Yarrol Province. A bimodal granite-gabbro intrusion; has an almost complete 2km-wide ring of mafic rocks. Local gradational contacts suggest the mafic phase was not entirely solid when intruded. Probably comagmatic with Rookwood Volcanics.||||Intrudes Balaclava Formation and Youlambie Conglomerate.|A zoned pluton; a rim of biotite-hornblende diorite, and quartz diorite; and a core of A-type leucocratic hornblende granite; brecciated and net-veined contacts between core and margin. Minor aplite.|
39147|Kyle Mohr Igneous Complex|73197|6|Mentioned|p475 Fig.6, 476|Guadalupian|Guadalupian|New England Orogen, northern. Considered coeval with Rookwood Volcanics.|270 Ma||||Bimodal intrusives.|
23709|La Villa Igneous Complex|22847|3|Fully described|p 46||Late Ordovician|||||||
23709|La Villa Igneous Complex|23422|5|Briefly described|p214 Table 6.8|||||||||
23709|La Villa Igneous Complex|23513|5|Briefly described|Map legend|Silurian|Ordovician|Palaeozoic Intrusive No. 451.||||||
23709|La Villa Igneous Complex|42633|5|Briefly described|Table 1 P10|||Reserved.||||||
23709|La Villa Igneous Complex|42750|2|Defined|p38|Early Silurian|Ordovician|||||||
23709|La Villa Igneous Complex|43093|4|Described|Appendix 1|Late Ordovician|Ordovician|Middle to Late Ordovician||||||
23709|La Villa Igneous Complex|43259|4|Described|Appendix 1,p48.|Early Silurian|Ordovician|||||||
23709|La Villa Igneous Complex|43934|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
23709|La Villa Igneous Complex|62521|6|Mentioned|p15|||Geological Province: Ravenswood Batholith. Mixtures of Hogsflesh Creek Granodiorite and gabbro and diorite are well-developed adjacent to contacts. Contains hornblende-bearing gabbros. Mafic intrusive rocks.||||||14-JAN-08
78364|Lady Clayre Formation|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Mary Kathleen Domain, Mount Isa Inlier. Isa Superbasin. See also references to Lady Clayre Dolomite (Solid Geology Map, Mount Isa Block Time-Space Plot; p15, p26).||Mount Albert Group.|||Dolomitic, locally pyrrhotitic siltstone, silty to sandy dolostone and fine-grained variably dolomitic sandstone.|
78364|Lady Clayre Formation|69056|5|Briefly described|p55, Time-Space plot sheet|Statherian|Statherian|Also appears as Lady Clayre Dolomite on Time-Space plot sheet. Maximum depositional age.|1691 +/- 9 Ma (Carson et al., 2011).|Upper Mount Albert Group.||Overlies Coocerina Formation. Time-equivalent of Mount Roseby Schist. Possibly correlated with the Gun Supersequence.||
78364|Lady Clayre Formation|69591|4|Described|p45, p56|||Mary Kathleen Domain, Mount Isa Province. Part of Gun Supersequence. Deep marine deposits. See also reference to [superseded] Lady Clayre Dolomite (p43 Fig.2.31).|1691 +/- 9 Ma (MDA: Carson et al., 2011).|Mount Albert Group.||Overlies Knapdale Quartzite. Probably correlates with Mount Isa Group.|Dolomitic, locally pyrrhotitic siltstone, silty to sandy dolostone and fine-grained variably dolomitic sandstone.|
78364|Lady Clayre Formation|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Dolomitic, locally pyrrhotitic siltstone and fine-grained variably dolomitic sandstone.|
78364|Lady Clayre Formation|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Dolomitic, locally pyrrhotitic siltstone and fine-grained variably dolomitic sandstone.|
78364|Lady Clayre Formation|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Overlies Coocerina Formation.|Separately mapped: dolomitic, locally pyrrhotitic siltstone and silty to sandy dolostone; grey fine-grained variably dolomitic sandstone and siltstone.|
78364|Lady Clayre Formation|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Subdidvided into two unnamed units.||Mount Albert Group|||Dolomitic, locally pyrrhotitic siltstone and silty to sandy dolostone; grey, fine-grained variably dolomitic sandstone and siltstone.|
78364|Lady Clayre Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1691+/-9 Ma (MDA: U-Pb zircon SHRIMP)||||Dolostone.|
78364|Lady Clayre Formation|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP age of 1691 +/- 9 Ma reported by Carson et al. (2011).|1691 +/- 9 Ma|||||
78364|Lady Clayre Formation|73529|5|Briefly described|p5|Statherian|Statherian|Calvert Superbasin, late. Deep marine setting. Misspelt Lady Clayre Foramtion p5.|1691+/-9 Ma maximum depositional age|Mount Albert Group||||
78364|Lady Clayre Formation|73553|5|Briefly described|p8 Fig.1.2.3, p228|Statherian|Statherian||1691+/-9 Ma MDA|Mount Albert Group||Is cut by Lakeview Dolerite||
75647|Lady Norman Granodiorite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, fine to medium-grained, slightly to moderately porphyritic, strongly foliated to gneissic hornblende-biotite granodiorite; with minor clinopyroxene locally, lenticular mafic inclusions up to c. 3 m long, and traces of titanite, allanite.|
22158|Lags Microgranite|23423|5|Briefly described|p315 Table 7.4||Early Permian|Age: 279 +/- 4 Ma.  Lags Supersuite.||||||
22158|Lags Microgranite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Age 279 +/-4 Ma Rb-Sr. Of Lags Supersuite.||||||07-APR-15
22158|Lags Microgranite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Age: 279+/-4 Ma, Rb-Sr. Of Lags Supersuite.||||||
22158|Lags Microgranite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 429. A-Type.||||||
22158|Lags Microgranite|23616|5|Briefly described|Table 3 p48, p80||Early Permian|Age: 279+/-4 Ma (Rb-Sr).||||||
22158|Lags Microgranite|23713|5|Briefly described|p71 Appendix 2, p29||Early Permian|Intrudes Early Permian units of the Featherbed Volcanic Group. Age: 279+/-4 Ma (Rb-Sr). Of Lags Supersuite.||||||
22158|Lags Microgranite|24485|5|Briefly described|p69 Tb.12|Early Permian|Early Permian|Age: 279 +/- 4Ma. Parent: Lags Supersuite||||||
22158|Lags Microgranite|43060|5|Briefly described|p113|||Age of 279+/-4 Ma.||||||
22158|Lags Microgranite|43083|5|Briefly described|p259|||Of Lags Supersuite. Age of 279+/-4 Ma. A-type.  Lithology included.||||||17-JUN-09
22158|Lags Microgranite|43087|5|Briefly described|p74|||||||||
22158|Lags Microgranite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Pale grey, pink or brown, strongly and abundantly porphyritic biotite microgranite.  Age: 279+/-4Ma.||||||15-JUN-06
22158|Lags Microgranite|43254|5|Briefly described|map legend||Early Permian|of Lags Supersuite. Age 279+/-4 Ma.||||||
22158|Lags Microgranite|43259|4|Described|Appendix 1,p46.||Early Permian|Age is 279+/-4 Ma.||||||
22158|Lags Microgranite|43625|6|Mentioned|p38|||||||||
22158|Lags Microgranite|43626|6|Mentioned|p11|||||||||
22158|Lags Microgranite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 279 +/- 4 Ma (Rb-Sr). Geological Province: Kennedy Province. Pale to medium grey, pink or brown, highly and abundantly porphyritic biotite microgranite.||||||31-MAY-04
22158|Lags Microgranite|60425|4|Described|p47 Tb. 3, p77, p182, p276-7 Appdx.|Early Permian|Early Permian|Of Lags Suite (Lags Supersuite). Age: 279+/-4Ma. Intrudes Tennyson Volcanic Subgroup (Featherbed Volcanic Group), Hodgkinson Fm. A-type. Pale to medium grey, pink, or brown, highly porphyritic to even-grained biotite microgranite.||||||07-APR-15
22158|Lags Microgranite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.|280 +/- 3 Ma (Rb-Sr total rock); 281 Ma (biotite).|Unit in Lags Supersuite.|||Pale to medium grey, pink or brown, highly and abundantly porphyritic biotite microgranite.|
22158|Lags Microgranite|69593|5|Briefly described|p484, p510|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 Ma.|Lags Suite.|||A-type.|
69318|Lags Suite|60425|5|Briefly described|p276-7 Appdx.|Early Permian|Early Permian|Of Lags Supersuite. Age: 280+/-4Ma (Bustlem) and 279+/-4Ma (Bustlem). Contains Lags and Yoka Microgranites and an unnamed highly porphyritic (hornblende-) biotite microgranite. A-type.||||||07-FEB-11
69318|Lags Suite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Lags Supersuite.|Lags, Yokas Microgranites.||A-type.|
28032|Laia Granite|23420|5|Briefly described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite.||||||
28032|Laia Granite|23496|5|Briefly described|Table 2, p40|Devonian|Silurian|of Aralba Suite, Kintore Supersuite. Inferred to predate Fish Creek Granite and cuts the Aralba Granite.||||||
28032|Laia Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Aralba Suite.||||||
28032|Laia Granite|43596|4|Described|p30, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite).  Intruded by Fish Creek Granite. White to buff, locally reddish-brown (ferruginised) med.-coarse, mostly mod'ly porphyritic (biotite-)muscovite leucogranite+K-feldspar and muscovite phenocrysts; deeply weathered.||||||27-JAN-09
28032|Laia Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
32276|Lakes Creek Formation|24420|5|Briefly described|p7|Early Permian|Early Permian|Of Berserker Group.||||||
32276|Lakes Creek Formation|24615|5|Briefly described|CD|Permian|Permian|[Pkl].  Siltstone and lithic sandstone.||||||
32276|Lakes Creek Formation|50207|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||
32276|Lakes Creek Formation|50209|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||17-MAY-04
32276|Lakes Creek Formation|50212|5|Briefly described|Map Legend|Permian|Permian|Of Berserker Group||||||
32276|Lakes Creek Formation|60557|5|Briefly described|p25|Early Permian|Early Permian|Well-bedded sequence of siltstone and sandstone, intruded by sills of basalt.||||||09-JUN-05
32276|Lakes Creek Formation|61778|3|Fully described|p233, p234 Fig. 1, p235, p240 Fig. 11||Early Permian|Of Berserker Group. Consists of interbedded marine siltstones and sandstones. Geological Province: Berserker Subprovince. See p235 for detailed lithology.||||||07-FEB-11
32276|Lakes Creek Formation|64429|2|Defined|p15, p17-19|Early Permian|Early Permian|Basal unit of Berserker Group; lateral equivalent of Chalmers Formation; overlies Mount Alma Formation and Rockhampton Group. Thickness: ~800m. Grey, massive, indurated siltstone and sandstones, etc. Intruded by Ellrott Rhyolite.||||||
32276|Lakes Creek Formation|68008|2|Defined|p158-163, p166|Permian|Permian|Originally Lakes Creek beds of Smith (1887). Named after Lakes Creek, a tributary of the Fitzroy River. Detailed study was done by East (1946). Defined here as Lakes Creek Formation; type area is a 1 km2 area bounded by Lakes Creek quarry and Nerimbera settlement. Previously a part of the Berserker Series (Whitehouse, 1930), renamed the Berserker beds (Kirkegaard et al., 1970), which was divided into the Berserker Group (Crouch and Parfrey, 1998) including this unit. Up to 800m thick. Early Permian marine fossils listed.||Basal Berserker Group.||Unconformably overlies Mount Alma Formation and Rockhampton Group. Partial equivalent of Chalmers Formation. Time-correlative of Yarrol Formation. Intruded by Ellrott Rhyolite.|A sequence of grey, massive, indurated siltstones and lithofeldspathic to quartzofeldspathic sandstones derived from felsic to intermediate volcanics, and chert. Local fossiliferous calcareous sandstone to limestone. Silicification common.|
32276|Lakes Creek Formation|68679|5|Briefly described|p350|||Berserker Subprovince, Yarrol Province. Similar to Chalmers Formation but without the latter's volcaniclastics and breccia.||Basal Berserker Group.||Laterally equivalent to upper part of Chalmers Formation.|Massive, grey, thin- to medium-bedded siltstone and fine- to medium-grained, well-sorted, lithofeldspathic to quartzofeldspathic sandstone derived from felsic to intermediate volcanics; minor chert, granule-pebbly sandstone, calc. sst to limestone.|
25986|Lakeview Dolerite|22461|6|Mentioned|p468|||||||||
25986|Lakeview Dolerite|22462|6|Mentioned|P7||Stenian|Age of unit is 1100 Ma||||||
25986|Lakeview Dolerite|23324|6|Mentioned|p468 Fig.1|||||||||07-FEB-07
25986|Lakeview Dolerite|23519|5|Briefly described|p138|Mesoproterozoic|Mesoproterozoic|Age: 1116+/-12 Ma (Rb/Sr). Geological Province: Mt Isa Inlier.||||||
25986|Lakeview Dolerite|24111|6|Mentioned|p211|||||||||
25986|Lakeview Dolerite|24115|5|Briefly described|p31 Fig. 28|Mesoproterozoic|Mesoproterozoic|Age: 1116 +/- 12 ( Rb-Sr). Geological Province: Mount Isa Inlier.||||||
25986|Lakeview Dolerite|24535|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Block.||||||07-NOV-08
25986|Lakeview Dolerite|30601|6|Mentioned|p419|||||||||
25986|Lakeview Dolerite|33900|6|Mentioned|p30|||Redating||||||
25986|Lakeview Dolerite|35074|6|Mentioned|Fig.2|||||||||
25986|Lakeview Dolerite|35167|2|Defined|p155|Late Precambrian|Late Precambrian|||||||
25986|Lakeview Dolerite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
25986|Lakeview Dolerite|36052|6|Mentioned|Fig.1|||||||||
25986|Lakeview Dolerite|37818|6|Mentioned|p78|||||||||
25986|Lakeview Dolerite|39049|4|Described|p843|||||||||
25986|Lakeview Dolerite|39445|5|Briefly described|Table 3|||See P56 1140+ or - 20 Ma. See also p43 and Table 3.||||||09-FEB-09
25986|Lakeview Dolerite|39622|6|Mentioned|p28|||See also Fig.2||||||
25986|Lakeview Dolerite|39799|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25986|Lakeview Dolerite|41957|5|Briefly described|p66|||||||||
25986|Lakeview Dolerite|42706|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Age: ~1116Ma.||||||09-FEB-09
25986|Lakeview Dolerite|42858|5|Briefly described|p671|||||||||
25986|Lakeview Dolerite|43643|5|Briefly described|p609|||Rb-Sr age: 1115 Ma.||||||09-FEB-09
25986|Lakeview Dolerite|45161|6|Mentioned|p14|||See also P53||||||
25986|Lakeview Dolerite|45166|5|Briefly described|p40|||||||||
25986|Lakeview Dolerite|46962|6|Mentioned|p254|||||||||
25986|Lakeview Dolerite|46976|6|Mentioned|p98|||||||||
25986|Lakeview Dolerite|61924|5|Briefly described|p44|Mesoproterozoic|Mesoproterozoic|Age: 1116+/-12 Ma. Geological Province: Mary Kathleen Belt.||||||
25986|Lakeview Dolerite|61936|6|Mentioned|p201|Mesoproterozoic|Mesoproterozoic|East-west oriented dykes.  Age: ca1115Ma. ||||||
25986|Lakeview Dolerite|62428|5|Briefly described|p351 Tb. 6|Mesoproterozoic|Mesoproterozoic|Age: 1116+/-12Ma (Rb-Sr). Palaeomagnetic data. Presented informally as Lakeview dolerite.||||||10-FEB-09
25986|Lakeview Dolerite|63114|6|Mentioned|p1251, p1268, p1270.|||Emplaced at the time of assemblage of the Rodinia supercontinent.|c.1150 Ma.|||||
25986|Lakeview Dolerite|65396|5|Briefly described|p319|||Mount Isa Inlier. Unmetamorphosed dykes cutting the Williams-Naraku batholith, all regional structures and rock types.|1116 +/- 12 Ma (Rb-Sr: Page, 1983).|||||
25986|Lakeview Dolerite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Appears as Lakeview dolerite. Northeast-trending dykes in the Mount Isa Province. Produced in the Mordor Event, ME 23 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1135 Ma.|||||
25986|Lakeview Dolerite|66913|6|Mentioned|p188||||1116+/-12 Ma|||||
25986|Lakeview Dolerite|69003|5|Briefly described|p48 Fig.57|Mesoproterozoic|Mesoproterozoic|North Australian Craton. Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|1140 Ma.|||||
25986|Lakeview Dolerite|69591|5|Briefly described|p53|||Derrick, Wilson and Hill (1978). Forms undeformed NE-striking dykes cutting across late-Isan structures.|1116 +/- 12 Ma (Page, 1988).|||||
25986|Lakeview Dolerite|70355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Relatively unmetamorphosed pyroxene-bearing dolerite.|
25986|Lakeview Dolerite|70356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Relatively unmetamorphosed pyroxene-bearing dolerite.|
25986|Lakeview Dolerite|72684|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Overlies part of Mary Kathleen Domain, shown as younger than the Isan Orogeny (1590-1500 Ma).|||||Relatively unmetamorphosed pyroxene-bearing dolerite.|
25986|Lakeview Dolerite|72685|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Overlies part of Mary Kathleen Domain, shown as younger than the Isan Orogeny (1590-1500 Ma).|||||Relatively unmetamorphosed pyroxene-bearing dolerite.|
25986|Lakeview Dolerite|73137|6|Mentioned|p30||||||||Includes doleritic/gabbroic rocks.|
25986|Lakeview Dolerite|73553|4|Described|p145-146, p164, p173, p177,|Stenian|Ectasian|Youngest known mafic intrusives in the Mary Kathleen Domain. Formerly mapped as unnamed dolerite unit 'do6' before formal definition and detailed description by Derrick et al., (1978). Described in detail by Ellis and Wyborn (1984) who assign it to their 'E4' group. Tholeiitic. The unit is overall topographically recessive. Moderate magnetic response, less distinct in radiometric images. See also p110, p141, p145, p178 Tb.5.9.2, p182, p185, p188-189, p191-192, p194, p197-198, p224-232, p267.|1116+/-12 Ma Rb-Sr, ~1380 Ma K-Ar biotite|||Intrudes/cuts the Corella, Argylla, and Lady Clayre formations, Mount Roseby Schist, Myubee Igneous Complex, Lunch Creek Gabbro, Bushy Park Gneiss, Burstall, Overlander, and Winston Churchill granites|Series of a mafic dykes comprising a fine-grained, chilled margin and a coarser grained ophitic or sub-ophitic core. Shows no evidence of regional metamorphism.|03-FEB-23
30726|Lalor beds|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|1758+/-4Ma, 1762+/-3Ma||||||
30726|Lalor beds|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1760Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30726|Lalor beds|50332|6|Mentioned|p21|Proterozoic|Proterozoic|Informal name. Of the "Tommy Creek beds".||||||07-FEB-11
30726|Lalor beds|50536|5|Briefly described|p1.5, 11.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Tommy Creek Suite. Age: ~1760Ma.||||||
30726|Lalor beds|65505|6|Mentioned|980|Proterozoic|Proterozoic|Informal. Tommy Creek Block, east of Mary Kathleen Fold Belt. Crystallisation ages of 1762 +/- 5 Ma and 1758 +/- 4 Ma.||||||
30726|Lalor beds|67323|5|Briefly described|p16|||Wyborn et al. (2001). Based on zircon SHRIMP ages, included felsic metavolcanics previously assigned to Tommy Creek Microgranite (Derrick, 1980) or Tommy Creek beds (Hill et al., 1992). Now assigned to the Bulonga Volcanics.||||||
30726|Lalor beds|72596|6|Mentioned|p24|Statherian|Statherian|Geochronologic constraint from a rhyolite within the unit, see Geoscience Australia, 2011: Sample ID 95208051.|1758 +/- 4 Ma||||Includes rhyolite.|
29675|Lamdina beds|42999|5|Briefly described|Table 2 p90|Late Triassic|Late Triassic|Paly zone T4.||||||09-APR-15
36484|Lancewood Rhyolite|23291|5|Briefly described|p97 Tb. 3.11|Carboniferous|Carboniferous|Of the Newcastle Range I-types. Thickness: 1000-2000m. Geological Province: Georgetown Region.||||||08-JUL-15
36484|Lancewood Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 60.  I-Type.||||||
30108|Landers Igneous Complex|22847|3|Fully described|p 47|Early Permian|Ordovician|||||||
30108|Landers Igneous Complex|23504|5|Briefly described|Map Legend|Permian|Ordovician|||||||
30108|Landers Igneous Complex|43093|4|Described|Appendix 1|Early Permian|Ordovician|Ordovician to Early Permian age.||||||
30108|Landers Igneous Complex|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
24353|Lane Creek Formation|22533|6|Mentioned|p55|||In Georgetown Region||||||
24353|Lane Creek Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Mount Norna Quartzite and Broken Hill Cartwrights Creek Metasediments.||||||07-NOV-08
24353|Lane Creek Formation|23032|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24353|Lane Creek Formation|23220|5|Briefly described|p10|||Of the Etheridge Group.||||||16-JAN-07
24353|Lane Creek Formation|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Geological Province: Georgetown Region.||||||18-JUN-15
24353|Lane Creek Formation|23430|5|Briefly described|p450|||Of Etheridge Group. In Etheridge Province.||||||16-JAN-07
24353|Lane Creek Formation|23431|5|Briefly described|p530.|||In Forsayth Subprovince.||||||16-JAN-07
24353|Lane Creek Formation|23510|5|Briefly described|Map Legend||Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
24353|Lane Creek Formation|24197|5|Briefly described|p77|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
24353|Lane Creek Formation|24485|5|Briefly described|p1, 21|Proterozoic|Proterozoic|Of the Robertson River Subgroup. Intruded by the Cobbold Metadolerite, age: 1656 +/- 2Ma (U-Pb SHRIMP zircon)||||||05-JUN-15
24353|Lane Creek Formation|38714|2|Defined|p188|Mesoproterozoic|Mesoproterozoic|||||||
24353|Lane Creek Formation|39495|6|Mentioned|p142|||||||||
24353|Lane Creek Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24353|Lane Creek Formation|39924|6|Mentioned|p341|||||||||
24353|Lane Creek Formation|41975|5|Briefly described|p436|||||||||
24353|Lane Creek Formation|42199|5|Briefly described|Table 1 P280|||||||||
24353|Lane Creek Formation|43664|4|Described|p27|||||||||
24353|Lane Creek Formation|43740|6|Mentioned|Fig.5,p45||Proterozoic|||||||
24353|Lane Creek Formation|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
24353|Lane Creek Formation|50199|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
24353|Lane Creek Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Overlies: Corbett Formation. Underlies: Townley Formation. Intruded by Cobbold Metadolerite.||||||02-JUL-15
24353|Lane Creek Formation|50211|4|Described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Robertson River Subgroup (Etheridge Group). Conformably overlies Corbett Formation.||||||07-NOV-08
24353|Lane Creek Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||30-JUL-04
24353|Lane Creek Formation|50595|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup. Overlies: Corbett Formation. Underlies: Townley Formation.||||||02-JUL-15
24353|Lane Creek Formation|61258|6|Mentioned|p399|||||||||
24353|Lane Creek Formation|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
24353|Lane Creek Formation|65887|5|Briefly described|p41, p44, p47|Statherian|Paleoproterozoic|Of Robertson River Subgroup. Overlies Corbett Formation. Cobbold Metadolerite sill intruding Lane Creek Formation dated at 1656+/-2 Ma (Black et al., 1998).||||||
24353|Lane Creek Formation|66526|5|Briefly described|p4, p36. |Proterozoic|Proterozoic|Georgetown Province of the North Australian Crustal Element. Intruded by  c.1655 Ma. dolerite sills and basalt produced in the Lane Creek Event, ME 14 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|>1655 Ma.|||||
24353|Lane Creek Formation|66529|5|Briefly described|p22 |Mesoproterozoic|Mesoproterozoic|Forms basement to the Maureen uranium deposit.|||||Original sediments consisted of laminated, highly carbonaceous mudstone and siltstone, interbedded with pale grey to white mudstone and siltstone. Metamorphosed to mica schists with some quartzite and calc-silicate rocks.|
24353|Lane Creek Formation|66800|5|Briefly described|p926 Table 1, p928, pp932-933.|||Greenschist to upper amphibolite facies metamorphism; blastophytic amphibole and plagioclase laths persist locally. No mafic rocks occur above this unit in the upper part of Etheridge Group. Intruded by a dated leucogabbro sill.|1655.9 +/- 2.2 Ma.|Unit in Robertson River Subgroup.||Overlies Corbett Formation.|Metadolerite and metagabbro sills and small stocks common; mostly massive, but layering present in some sills.|
24353|Lane Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Georgetown-Coen-Yambo Inliers.|~1660-1650 Ma.|Lower Etheridge Group.|||Mudstone and siltstone.|
24353|Lane Creek Formation|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||Overlies Corbett Formation.||
24353|Lane Creek Formation|67430|6|Mentioned|p25, 60|Mesoproterozoic|Mesoproterozoic|Forms basement below the Maureen U deposit unconformity.|||||Mica schists with some quartzite and calc-silicate rocks. Produced by metamorphism of laminated, highly carbonaceous mudstone and siltstone, interbedded with pale grey to white mudstone and siltstone; local pure, recrystallised limestone beds.|
24353|Lane Creek Formation|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Robertson River Subgroup.|||Carbonaceous mudstone.|12-MAY-15
24353|Lane Creek Formation|68352|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Conformably overlies Corbett Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Townley Formation.|Mudstone and siltstone, commonly carbonaceous, locally calcareous; minor sandstone; grades into mica schist (commonly graphitic +/- andalusite, cordierite, sillimanite), quartzite and calc-silicate rocks.|
24353|Lane Creek Formation|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1650 Ma.|Unit in Robertson River Subgroup.||Conformably overlies Corbett Formation. Is intruded by Cobbold Metadolerite. Is overlain conformably by Townley Formation.|Mica schist (commonly graphitic +/- andalusite, cordierite, sillimanite), quartzite and calc-silicate rocks; grades into mudstone and siltstone, commonly carbonaceous, locally calcareous, minor sandstone; carbonaceous mudstone, phyllite and schist.|
24353|Lane Creek Formation|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1650 Ma.|Unit in Robertson River Subgroup.||Conformably overlies Corbett Formation. Is intruded by Cobbold Metadolerite.|Mica schist (commonly graphitic +/- andalusite, cordierite, sillimanite), quartzite and calc-silicate rocks.|
24353|Lane Creek Formation|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.|c.1650 Ma.|Unit in Robertson River Subgroup.||Conformably overlies Corbett Formation.|Carbonaceous mudstone.|
24353|Lane Creek Formation|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes 4 separately mapped facies variants.||Of the Robertson River Subgroup.||Intruded by the Cobbold Metadolerite. Conformably overlies Corbett Formation. Is overlain conformably by Townley Formation.|Mudstone and siltstone, commonly carbonaceous, locally calcareous, minor sandstone, grades into mica schist (commonly graphic +/- andalusite, cordierite, sillimanite), quartzite and calc-silicate rocks; carbonaceous mudstone; phyllite and schist.|
24353|Lane Creek Formation|68576|5|Briefly described|Q_11: p27-28|Paleoproterozoic|Paleoproterozoic|Georgetown area. Intrusion was probably soon after deposition as it does not extend into the conformably overlying units.||Etheridge Group.||Is intruded by Cobbold Metadolerite.|Mostly fine-grained metasedimentary rocks (including metasiltstone and mica schist); commonly carbonaceous (producing greyish soil). Lower amphibolite facies metamorphism; chiastolite porphyroblasts are relatively common.|
24353|Lane Creek Formation|69582|6|Mentioned|p76|||Etheridge Province. Intersected in GSQ Georgetown 8-9R.||Robertson River Subgroup||||
24353|Lane Creek Formation|69591|4|Described|p61-62, p65, p67-68, p82-83, p108|Paleoproterozoic|Paleoproterozoic|Forsayth Subprovince, Etheridge Province. Uppermost unit in the Group. Up to 2000m thick. Metadolerite and metagabbro sills common. Contains rare detrital zircons aged ~1695 Ma (Neumann and Kositcin, 2011). Detrital zircon spectra. This ~1656 Ma age, by Black et al. (1998) is of a leucogabbro sill.|1656 +/- 2 Ma (minimum age).|Robertson River Subgroup.||Is overlain by Townley Formation. Is intruded by Cobbold Metadolerite. Locally interfolded with Corbett and Townley Formations.|Mainly laminated, commonly highly carbonaceous mudstone and siltstone; locally calcareous or dolomitic; rare, thin, relatively pure recrystallised limestone beds. Grades eastwards into mica schist, some quartzite and minor calc-silicates.|
24353|Lane Creek Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Georgetown area.|ca 1675-1650 Ma|||Overlies the Dead Horse Metabasalt.|Siltstone, carbonaceous shale and dolomite.|
24353|Lane Creek Formation|72297|5|Briefly described|p712, p718|||About 30km SW of Georgetown.|||||Metasediments with pegmatite dykes containing lithium (in lepidolite and amblygonite) with tantalite, cassiterite and ilmenite, adjacent to greisenised granite.|
27274|Lang Creek Granite|42304|2|Defined|p24|Permian|Carboniferous|Reserved April 1988 by R.J. Bultitude.||||||02-JUN-09
27274|Lang Creek Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
27274|Lang Creek Granite|60425|4|Described|p276-7 Appdx.|Early Permian|Early Permian|Of Whypalla Suite (Whypalla Supersuite). S-type. White to cream, medium-grained, even-grained (garnet-) biotite-muscovite granite.||||||07-FEB-11
27274|Lang Creek Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Suite.||||
41803|Langdale Hill Rhyolite|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Greenish grey to grey, cyrstal rich rhyolitic ignimbrite, locally containing lithic clasts and fiamme; some rhyolite flows.||||||
41803|Langdale Hill Rhyolite|65388|2|Defined|p129-130; p86 Fig.35; p86, 143|Early Permian|Early Permian|Of Lizzie Creek Volcanic Group. Transgressively overlies Mount Benmore Volcanics, Tartrus Rhyolite, suggesting an unconformity. Carmila beds unconformably overlie. Possible time correlative of  Mount Buffalo Volcanics. Forms rugged, hilly topography and is well exposed. Mostly yellowish to bluish grey crystal-rich rhyolitic ignimbrite. Sequence of flows. Misspelt as Langdale Rhyolite p113, 143. ||||||
41803|Langdale Hill Rhyolite|68679|5|Briefly described|p358|||A thick pile of rhyolitic volcanics near Tooloombah homestead, Connors Subprovince. Possible accumulation within a local cauldron. Thickness is unknown. Relationships suggest early Permian.||||Transgressively (?unconformably) overlies Mount Benmore Volcanics and Tartrus Rhyolite. Is overlain unconformably by Carmila beds. May correlate with Mount Buffalo Volcanics.|Mostly crystal-rich rhyolitic ignimbrite with lithic clasts and flattened fiamme; extensive areas of argillic alteration common.|
27818|Langdon River Mudstone|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Etheridge Group.  Mudstone and phyllite, rare sandstone and siltstone.||||||
27818|Langdon River Mudstone|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Willyama Supergroup Dalnit Bore Metasediments and the Mt Isa Soldiers Cap Group.||||||07-NOV-08
27818|Langdon River Mudstone|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon). Thickness: 800-1400m. Geological Province: Georgetown Region.||||||08-JUL-15
27818|Langdon River Mudstone|23430|5|Briefly described|p456.|||||||||
27818|Langdon River Mudstone|38716|4|Described|p193|||||||||
27818|Langdon River Mudstone|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27818|Langdon River Mudstone|39924|6|Mentioned|Fig.3|||||||||
27818|Langdon River Mudstone|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27818|Langdon River Mudstone|41975|6|Mentioned|p437|||||||||
27818|Langdon River Mudstone|42199|5|Briefly described|Table 1 P280|||||||||
27818|Langdon River Mudstone|43664|4|Described|p36|||||||||
27818|Langdon River Mudstone|43729|6|Mentioned|p17|||||||||
27818|Langdon River Mudstone|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.  Overlies: Candlow Formation.||||||07-NOV-08
27818|Langdon River Mudstone|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||30-JUL-04
27818|Langdon River Mudstone|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Etheridge Group. Overlies: Candlow Formation.||||||07-NOV-08
27818|Langdon River Mudstone|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Etheridge Group.  Cleaved mudstone and phyllite, cross-laminated micaceous fine quartz sandstone and sandy siltstone.||||||
27818|Langdon River Mudstone|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
27818|Langdon River Mudstone|66800|6|Mentioned|p926 Table 1.|||||||Overlies Candlow Formation.||
27818|Langdon River Mudstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||Upper Etheridge Group.||||
27818|Langdon River Mudstone|67341|5|Briefly described|vi, p22-25|||Forsayth Subprovince, Etheridge Province. Maximum depositional age.|1629 +/- 12 Ma (SHRIMP U-Pb zircon).||||Includes dark grey, fine-grained sandstone-mudstone with planar laminations.|
27818|Langdon River Mudstone|67430|6|Mentioned|p25|||||||||
27818|Langdon River Mudstone|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Candlow Formation.|Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|12-MAY-15
27818|Langdon River Mudstone|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Candlow Formation.|Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|12-MAY-15
27818|Langdon River Mudstone|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Min Age: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Candlow Formation.|Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|18-MAY-15
27818|Langdon River Mudstone|68355|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Candlow Formation.|Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|04-JUN-15
27818|Langdon River Mudstone|68356|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.|||Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|04-JUN-15
27818|Langdon River Mudstone|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Etheridge Group.||Unconformably overlain by the Langlovale Group. Conformably underlain by the Candlow Formation.|Laminated maroon and grey variably carbonaceous and pyritic mudstone; minor siltstone and fine micaceous quartzose sandstone.|
27818|Langdon River Mudstone|69591|4|Described|p61-62, p66, p68, p82-83|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. Up to 1500m thick. Suggested depositional environments include deep-water sediments or turbidites. Detrital zircon spectra.|~1640 Ma.|Uppermost Etheridge Group.||Is intruded by the Forest Home Trondhjemite.|A distinctive laminated mudstone that is red and grey in outcrop but probably strongly carbonaceous and pyritic at depth.|
27818|Langdon River Mudstone|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1629+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
28247|Langlovale Group|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Yarman Formation, Malacura Sandstone.||||||
28247|Langlovale Group|22533|6|Mentioned|p54|Statherian|Statherian|Placed in Forsyth subprovince.||||||16-JAN-07
28247|Langlovale Group|22669|6|Mentioned|P248, Fig1||Mesoproterozoic|||||||
28247|Langlovale Group|22811|6|Mentioned|p605|||In the Forsayth Subprovince.||||||16-JAN-07
28247|Langlovale Group|23291|3|Fully described|p26, p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|See also Langlo Vale Group. Age: ~1550Ma. Intruded by Esmeralda Supersuite. Overlain by Eulo Queen Group; underlain by Etheridge Group. Geological Province: Georgetown Region.||||||02-JUL-15
28247|Langlovale Group|23420|6|Mentioned|p 136|||In the Forsayth Subprovince.||||||
28247|Langlovale Group|23430|5|Briefly described|p450|||Underlain by Etheridge Group - unconformable contact.  In Etheridge Province.||||||16-JAN-07
28247|Langlovale Group|23431|5|Briefly described|p531|||||||||
28247|Langlovale Group|23453|5|Briefly described|p10 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
28247|Langlovale Group|24197|5|Briefly described|p76, p78|Paleoproterozoic|Paleoproterozoic|Fluviatile to marine, pro-deltaic deposits.Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
28247|Langlovale Group|38716|2|Defined|p193|Mesoproterozoic|Mesoproterozoic|Age between 1550 and 1560Ma because overlying Croydon Volcanic Group dated at 1552+/-2Ma in 1990.||||||13-MAY-15
28247|Langlovale Group|39495|6|Mentioned|p142|||||||||
28247|Langlovale Group|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28247|Langlovale Group|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28247|Langlovale Group|40659|6|Mentioned|p248|||Mention p253.||||||16-JAN-07
28247|Langlovale Group|40860|6|Mentioned|Fig.1|||||||||
28247|Langlovale Group|41975|5|Briefly described|p437|||||||||
28247|Langlovale Group|43595|5|Briefly described|p353|||Post-dates 1570 Ma||||||
28247|Langlovale Group|43664|5|Briefly described|p53-54||Mesoproterozoic|||||||
28247|Langlovale Group|43729|5|Briefly described|p1||Mesoproterozoic|||||||
28247|Langlovale Group|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes: Malacura Sandstone.||||||
28247|Langlovale Group|50537|6|Mentioned|p1.1|||Geological Province: Georgetown Inlier.||||||
28247|Langlovale Group|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes the Malacura Sandstone.||||||05-JUL-04
28247|Langlovale Group|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Yarman Formation and Malacura Sandstone.||||||
28247|Langlovale Group|61258|5|Briefly described|p386, p387 Fig. 1|Mesoproterozoic|Mesoproterozoic|See also Croydon Volcanics. Fluvial to marine deposits. Geological Province: Georgetown Inlier.||||||
28247|Langlovale Group|61924|5|Briefly described|p49 Fig.6|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier.||||||
28247|Langlovale Group|63866|5|Briefly described|p75, p77, p79, p81|||Forsayth Subprovince, Etheridge Province.|||Includes the Malacura Sandstone and the Yarman Formation.|Unconformably overlies the Etheridge Group. Overlain by the Croydon Volcanics.  Intruded by the Esmeralda Supersuite.||
28247|Langlovale Group|65887|5|Briefly described|p40 Fig.1|Mesoproterozoic|Mesoproterozoic|||||||
28247|Langlovale Group|66529|5|Briefly described|p5 |||Western Etheridge Province. Much lower metamorphic grade (greenschist and sub-greenschist facies) than rocks in the eastern part of the Province (amphibolite and granulite facies). Maximum depositional age, continuing until 1590 Ma.|~1625 Ma (Withnall et al., 1997, 2009).|||Unconformably overlies the Etheridge Group. Unconformably overlain by the Croydon Volcanic Group.|Sandstone, mudstone and shale.|
28247|Langlovale Group|66800|6|Mentioned|p925.|||Fluvial to marine, pro-deltaic deposits.||||||
28247|Langlovale Group|67323|5|Briefly described|p21, p37|||Georgetown Inlier. Deposited unconformably on metamorphic basement.|~1570-1550 Ma.|||Unconformably overlies Etheridge Group. Is overlain by Croydon Volcanic Group. May correlate with Canobie Sequence.||
28247|Langlovale Group|67341|6|Mentioned|p25|||Etheridge Province.|||Malacura Sandstone.|||
28247|Langlovale Group|67430|6|Mentioned|p25|||||||||
28247|Langlovale Group|68307|5|Briefly described|p78, p81, p85, p87-88, p97|Mesoproterozoic|Mesoproterozoic|Etheridge Province. North Australian Craton. Up to c.3km thick. Occurs to a depth of about 7.5km; is subhorizontal and seismically very non-reflective.||||||
28247|Langlovale Group|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.|||Includes Malacura Sandstone and Yarman Formation.|||
28247|Langlovale Group|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.|||Includes Malacura Sandstone and Yarman Formation.|||
28247|Langlovale Group|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.|||Includes Malacura Sandstone.|||
28247|Langlovale Group|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.|||Includes Malacura Sandstone.|||
28247|Langlovale Group|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.|||Includes Malacura Sandstone.|||
28247|Langlovale Group|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Savannah Province. Shown as older than D2 (~ 1550-1560 Ma) and younger than D1 (> 1560 Ma , < 1590? Ma).|~ 1590?-1550 Ma||Includes Malacura Sandstone.|Unconformably underlain by the Langdon River Mudstone.||
28247|Langlovale Group|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28247|Langlovale Group|68576|6|Mentioned|Q_11: p2|||||||||
28247|Langlovale Group|69591|5|Briefly described|p48, p61-62, p68-70, p75-76, p83, p109|||Withnall and Mackenzie (1980, 1983); Withnall (1996). Georgetown Inlier, Forsayth Subprovince, Etheridge Province; ?part of the Savannah Province. Detrital zircon spectra: MDA of ~1625 Ma.|>1550 Ma.||Malacura Sandstone, Yarman Formation.|Unconformably overlies the Etheridge Group. Is overlain unconformably by and faulted against the Croydon Volcanic Group and is intruded by the Esmeralda Supersuite.||
28247|Langlovale Group|70207|6|Mentioned|p14|Mesoproterozoic|Mesoproterozoic|Georgetown region.||||||
36349|Langton Dolerite|23251|6|Mentioned|Table 2 p18|||Of Arnold 1996. Discordant body within Upper Nash Clastics.  See also p42.||||||21-JUN-06
36349|Langton Dolerite|23542|4|Described|p388-389|||Dolerite sill within Gympie Group. Also see p380.  Of South Curra Limestone.||||||25-NOV-05
36349|Langton Dolerite|61780|4|Described|p257, p258, p259, p263|Late Permian|Middle Permian|Thickness: <100m. Distinctively amygdaloidal olivine-bearing alkaline dolerite (continental) with ohphitic textures.||||||
36349|Langton Dolerite|70913|3|Fully described|p7, p8 fig 3, p20-p24, p76, p77, p79|Late Permian|Middle Permian|Gympie Province. Name derived from Langton Road West of the Scotland Shaft, Gympie. Reference drill holes named. Distribution briefly discussed. Maximum thickness of 70m, on average between 10-20m thick. Shown as Member of South Curra Limestone p8, but unit relationships are enigmatic since it variably occurs beneath the South Curra Limestone or the Glanmire Conglomerate. See also p25, 67, 69, 71, Appendix 1 maps.||Previously of South Curra Limestone. Now stand alone Formation- level unit in Gympie Group.||Overlies the Highbury Basalt. Appears to intrude as a sill into South Curra Limestone and Glanmire Conclomerate.|Massive fine-grained dolerite, partly amygdaloidal. Composed of randomly interlocking laths of plagioclase which may be altered. The interstitial groundmass consists of fine quartz, albite, chlorite, clays, sericite and patches of carbonates.|28-FEB-19
81118|Langton Dolomite|69599|5|Briefly described|p592|Pleistocene|Pliocene|Informal name. Capella-Clermont district. Up to 13m thick. Postdates Miocene silcrete and overlies Clermont basalt flows. The limestone probably represents calcrete weathering profiles and/or small ponded areas in the local broad drainage plain.|||||Calcretes and magnesian limestone.|
28668|Langtry Gully Member|30451|5|Briefly described|p16|||See also Fig.2||||||
28668|Langtry Gully Member|31999|5|Briefly described|Table 1|||||||||
28668|Langtry Gully Member|32141|6|Mentioned|p145|||||||||
28668|Langtry Gully Member|32865|6|Mentioned|p479|||Fauna. Davies Range Fm.||||||
28668|Langtry Gully Member|44379|2|Defined|p3-8,24,Tb.1,3,map||Late Devonian|Unit of Dawes Range Formation.||||||
25726|Lankelly Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Lankelly Suite||||||
25726|Lankelly Granite|22781|4|Described|p30|Paleozoic|Paleozoic|Lankelly Suite||||||07-NOV-08
25726|Lankelly Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Lankelly Suite of the Kintore Supersuite. Intrudes Coen Metamorphic Group. Age: 407+/- 5Ma||||||
25726|Lankelly Granite|42610|1|Redefined|p18|Early Devonian|Late Silurian|Redefinition of the "Lankelly Adamellite". Age 407+/-7 to 408+/-6Ma.||||||
25726|Lankelly Granite|43738|6|Mentioned|p5|||||||||
25726|Lankelly Granite|43741|3|Fully described|p8|Devonian|Silurian|Ages(U-Pb): 407+/-4 Ma, 411+/-11 Ma||||||
25726|Lankelly Granite|69592|5|Briefly described|p282|||Cape York Peninsula Batholith.|408 +/- 6 Ma; 407 +/- 78 Ma (SHRIMP U-Pb zircon).|Kintore Supersuite.||||
25726|Lankelly Granite|71031|4|Described|p14, p20|Devonian|Devonian|Intruded by an unnamed feldspar-quartz porphyry dyke and an unnamed rhyolitic dyke on COEN (7570). At the contact of the granite and the unnamed feldspar-quartz porphyry gold mineralised quartz veins are found. The unnamed feldspar-quartz porphyry dyke has a dated magmatic crystallisation age of 284.2 +/- 2.1 Ma and the unnamed rhyolite dyke has an age of 285.4 +/- 2 Ma providing a minimum age for this unit. Dates provided are SHRIMP ages derived from Black et al, 1992a,b.|408 +/- 6 Ma and 407 +/- 7 Ma|||Intrudes the Coen Metamorphic Group.|Light to medium-grey muscovite-biotite granite.|
25726|Lankelly Granite|71592|5|Briefly described|Appendix A.|||Palma Igneous Province.|407+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
25726|Lankelly Granite|71849|3|Fully described|p3, p5, p8, p12, p15, p36, p70-71, p86|Devonian|Devonian|See also p94-102, p108, p130, p151-152, p154, p160-161, p184, p195. Previously the Lankelly Adamellite (Willmott et al. 1973) for highly porphyritic granitic rocks cropping out around Coen. NNW-trending belt, ~29km long and up to ~11km wide; main component of the Suite. Forms hills with boulders and tors, and extensive pavements. Geophysics described; lithologies and geochemistry in detail. Moderately to locally highly deformed; partly recrystallised in high-strain zones. Hosts the abandoned Great Northern (gold) mine. Typically contains abundant K-feldspar phenocrysts. U-Pb zircon SHRIMP ages by Black et al. (1992). Other (Cooper et al., 1975) ages given.|408 +/- 6 Ma and 407 +/- 7 Ma.|Lankelly Suite.||Intrudes Goolha-Goolha Schist and Penny Gneiss. Is intruded by Twin Humps Granite. Adjacent to (probably intruded by) Kintore Granite. Is overlain nonconformably by Falloch beds.|Grey, medium-grained, generally highly porphyritic muscovite-biotite and biotite-muscovite granite; some fine- to medium-grained slightly porphyritic muscovite-biotite monzogranite. Calc-alkaline to shoshonitic, peraluminous S-type.|
25726|Lankelly Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Lankelly Suite.|||Grey, moderately to highly deformed, medium-grained, porphyritic muscovite-biotite and biotite-muscovite granite; strongly aligned K-feldspar phenocrysts typically 3cm; fine to medium, seriate to slightly porphyritic muscovite-biotite monzogranite.|
36630|Lansdowne granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 486.  I-Type.||||||
22166|Lappa Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Tennyson Volcanic Subgroup of Featherbed Volcanic Group.||||||
22166|Lappa Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Tennyson Volcanic Subgroup.||||||
22166|Lappa Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. 123. I-Type.||||||
22166|Lappa Rhyolite|23616|5|Briefly described|Table 3 p48||Late Carboniferous|Of Tennyson Volcanic Subgroup.||||||
22166|Lappa Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Tennyson Volcanic Subgroup (Featherbed Volcanic Group).  Biotite rhyolitic ignombrite.||||||15-JUN-06
22166|Lappa Rhyolite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|of Koorboora Volcanic Subgroup.||||||
22166|Lappa Rhyolite|43567|5|Briefly described|Table 1,p400|||||||||
22166|Lappa Rhyolite|43626|2|Defined|p33|Early Permian|Late Carboniferous|between 289+/-7 Ma and 306+/-3 Ma||||||
22166|Lappa Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22166|Lappa Rhyolite|60425|5|Briefly described|p46 Tb. 3|Late Carboniferous|Late Carboniferous|Of Tennyson Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
22166|Lappa Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Tennyson Volcanic Subgroup.|||Dark grey to greenish or brownish grey, welded, moderately to very crystal-rich, biotite rhyolitic ignimbrite; some rhyolite clasts in places at base.|
69447|Lappa Suite|60425|5|Briefly described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of the O'Briens Creek Supersuite. Contains The Gorge Rhyolite and Opah Granite. I-type.||||||07-FEB-11
36303|Laragon Volcanics|23291|4|Described|p42, p92 Tb. 3.9|Early Permian|Carboniferous|Parent: Silent Creek Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
36303|Laragon Volcanics|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Silent Creek Volcanic Group.||||||
23716|Laroona Formation|23422|5|Briefly described|p180, p206 Table 6.3|Middle Devonian|Early Devonian|Of Wilkie Gray Group.  Previously included in the Fanning River Group.||||||
23716|Laroona Formation|23430|5|Briefly described|p505|||Of Wilkie Gray Group.||||||
23716|Laroona Formation|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|of Wilkie Gray Group.||||||
23716|Laroona Formation|23522|5|Briefly described|p258|Middle Devonian|Early Devonian|Same unit as Laroona Arkose.||||||
23716|Laroona Formation|23893|5|Briefly described|p15|Eifelian|Emsian|Geological Province: Camel Creek Subprovince. Of Wilkie Gray Group.||||||
23716|Laroona Formation|24610|6|Mentioned|p64|Emsian|Emsian|Geological Province: Burdekin Basin. Of Zhen (1991). Authors preferred use of name Laroona Arkose.||||||
23716|Laroona Formation|24611|5|Briefly described|p193|Emsian|Emsian|Conglomerate, micaceous sandstone and shale. Thickness in type section: 146.5m. Overlies Argentine Metamorphics non-conformably. Geological Province: Burdekin Basin. See also p194 Fig. 1 and p196 Fig. 2.||||||02-JUL-15
23716|Laroona Formation|24612|4|Described|p8|Emsian|Emsian|Overlain by Mount Podge Limestone. Underlain by Argentine Metamorphics (unconformable). Max. thickness: 150m. Previously of Big Bend Arkose, now of Fanning Group in the Mount Podge area. Conglomerate, micaceous sandstone and siltstone.||||||20-DEC-04
23716|Laroona Formation|24613|2|Defined|p9 Fig. 4, p12-13, Tb. 1|Emsian|Emsian|Of Fanning Group. Unconformable on Argentine Metamorphics; conformable below Mount Podge Limestone. Max.thickness:150m. Geological province: Burdekin Basin. Type section included. Pebbly conglomerate, sandstone, siltstone, sandy limestone (more detail).||||||07-FEB-11
23716|Laroona Formation|24614|6|Mentioned|p192|||Name offered as an alternative for Laroona Arkose.||||||07-FEB-11
23716|Laroona Formation|42690|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
23716|Laroona Formation|42933|5|Briefly described|Fig.94 p258|||Actually listed as just Laroona.||||||
23716|Laroona Formation|43095|5|Briefly described|Plate 2|||of Fanning River Group.||||||
23716|Laroona Formation|68350|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.||Unit in Wilkie Gray Group.||Is overlain conformably by Mount Podge Limestone.|Fine- to coarse-grained, calcareous, feldspathic sandstone, pebbly sandstone and calcareous granule to pebble conglomerate; minor fossiliferous sandy limestone.|
23716|Laroona Formation|68351|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.||Unit in Wilkie Gray Group.||Is overlain conformably by Mount Podge Limestone.|Fine- to coarse-grained, calcareous, feldspathic sandstone, pebbly sandstone and calcareous granule to pebble conglomerate; minor fossiliferous sandy limestone.|
23716|Laroona Formation|68731|5|Briefly described|p177 Fig 3.91, p183, p185 Tb 3.4|Lower Devonian|Lower Devonian|Burdekin Basin. < 150 m thick. Near shore transgressive fluvial to shoreface facies with conglomerate clasts derived from erosion of the underlying basement.||Of the Wilkie Gray Group.||Non-conformably underlain by the Argentine Metamorphics.|Comprises pebbly conglomerate, medium-grained to very coarse grained sandstone, very fine grained to medium- grained micaceous sandstone, siltstone, and uncommon limestone. Scattered bioclasts.|
22167|Larramore Metabasalt Member|23086|6|Mentioned|p668|||Hodgkinson Formation?||||||
22167|Larramore Metabasalt Member|23423|5|Briefly described|p232|||Hodgkinson Formation; Hodgkinson Province.||||||
22167|Larramore Metabasalt Member|23511|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Hodgkinson Formation||||||
22167|Larramore Metabasalt Member|43083|3|Fully described|p53 Tb 5, p68-9|||Of Hodgkinson Formation. Geological province: Hodgkinson Province. Comprises mainly metabasalt lava flows with numerous inter;ayered chert lenses.||||||17-JUN-09
22167|Larramore Metabasalt Member|43285|5|Briefly described|Map Legend|||age Late Silurian? to Late Devonian? Of Hodgkinson Formation.||||||
22167|Larramore Metabasalt Member|43625|4|Described|p19,26,30|||||||||
22167|Larramore Metabasalt Member|60357|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Geological Province: Hodgkinson Province. Of the Hodgkinson Formation.||||||
22167|Larramore Metabasalt Member|60358|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Of the Hodgkinson Formation. Metabasalt, minor chert. Geological Province: Hodgkinson Province.||||||18-AUG-04
22167|Larramore Metabasalt Member|60425|3|Fully described|p13, p26|Devonian|Devonian|Of Hodgkinson Formation.Mainly metabasalt lava flows + numerous interlayered chert lenses from ~2m to 30m thick. The sequence contains minor intercalated tuffaceous metsedimentary rocks containing basic volcanic detritus.Geol.prov: Hodgkinson Province||||||07-FEB-11
22167|Larramore Metabasalt Member|63140|6|Mentioned|p570-572.|Carboniferous|Devonian|Hodgkinson Province. ~3 km wide.||Hodgkinson Formation|||Metabasalt flows and interlayered chert lenses that commonly show a weak to prominent tectonic foliation.|
22167|Larramore Metabasalt Member|66852|6|Mentioned|p938 Fig.2.|||||Unit in Hodgkinson Formation.|||Metabasalt, minor chert.|
22167|Larramore Metabasalt Member|69030|6|Mentioned|p6|Devonian|Devonian|Chillagoe Subprovince, Hodgkinson Province. The rank of Member is omitted in the diagram.||Hodgkinson Formation.||||12-SEP-16
22167|Larramore Metabasalt Member|69592|5|Briefly described|p231 Fig.4.4, p232, p237, p248 Fig.4.32|Devonian|Silurian|Mossman Orogen, Palmer-Barron Subprovince, Hodgkinson Province. Regarded more as sedimentary and volcanic rock assemblages rather than stratigraphic units which imply superpositional relationships. Forms a narrow, elongate zone characterised by a mafic volcanic/chert association.||Hodgkinson Formation.|||Greenschist facies metamorphism in the chlorite and biotite zones.|
34129|Larry Creek Complex|22630|5|Briefly described|p37|||||||||
34129|Larry Creek Complex|22844|6|Mentioned|p37|||||||||
34129|Larry Creek Complex|23049|3|Fully described|p64|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
34129|Larry Creek Complex|23283|2|Defined|p29||Permian|||||||
34129|Larry Creek Complex|23508|5|Briefly described|Map Legend|Permian|Ordovician|||||||
22172|Lass O'Gowrie Granite|23423|6|Mentioned|p305 Table 7.4|||||||||
22172|Lass O'Gowrie Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
22172|Lass O'Gowrie Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 247. I-Type.||||||
22172|Lass O'Gowrie Granite|23616|6|Mentioned|Table 1C p44|||||||||
22172|Lass O'Gowrie Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supersuite).  Pink to pale grey, fine to coarse biotite granite, porphyritic in part; aplite. Age: 318?Ma.||||||15-JUN-06
22172|Lass O'Gowrie Granite|43626|6|Mentioned|p10||Late Carboniferous|||||||
22172|Lass O'Gowrie Granite|60425|4|Described|p45,  49 Tb. 3, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Herberton Suite (O'Briens Creek Supersuite). Age: ~314Ma (Rb-Sr). Unconform.below/faulted against Walsh Bluff Volcanics.Intruded Boonmoo Volcanic Subgroup. Biotite granite and subordinate aplitic biotite microgranite; I-type.More lith. detail incl'd||||||07-FEB-11
28273|Lassies Creek Gravels|32553|4|Described|p36|||||||||
28273|Lassies Creek Gravels|37607|6|Mentioned|Fig.7|||||||||
28273|Lassies Creek Gravels|39445|5|Briefly described|Table 14|||||||||
28273|Lassies Creek Gravels|44060|14|Not recorded|Map Legend|Pleistocene|Pliocene|||||||
28273|Lassies Creek Gravels|44061|4|Described|Table 6|Pleistocene|Pliocene|||||||
28273|Lassies Creek Gravels|48904|2|Defined|p67|Pleistocene|Pliocene|Plioc. - Pleist.||||||
28273|Lassies Creek Gravels|68351|5|Briefly described|Map legend.|Quaternary|Late Tertiary||||||Locally mottled, poorly consolidated sand, silt, clay, minor gravel; high-level alluvial deposits, generally dissected; fluviatile and colluvial pebbly feldspathic sandstone, grit, minor conglomerate.|
23717|Latan Granite|22847|3|Fully described|p 45|Ordovician|Early Ordovician|||||||
23717|Latan Granite|23422|6|Mentioned|p210 Table 6.6|||||||||
23717|Latan Granite|42633|5|Briefly described|Table 1 P9|||Reserved.||||||
23717|Latan Granite|42750|2|Defined|p38|Middle Ordovician|Early Ordovician|||||||
23717|Latan Granite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Early to Middle Ordovician||||||
23717|Latan Granite|43259|4|Described|Appendix 1,p49.|Early Devonian|Ordovician|age Ordivician (-Early Devonian).||||||
23717|Latan Granite|43934|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
25989|Lavery Creek Granite|22847|3|Fully described|p 39|Ordovician|Early Ordovician|||||||
25989|Lavery Creek Granite|23422|5|Briefly described|p172, p209 Table 6.6|Middle Ordovician|Middle Ordovician|Of Lavery Creek Supersuite.||||||
25989|Lavery Creek Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 87. I-Type.||||||
25989|Lavery Creek Granite|42633|5|Briefly described|Table1 P11|||Reserved as Lavery Creek Granodiorite.||||||
25989|Lavery Creek Granite|42750|2|Defined|p36|Middle Ordovician|Early Ordovician|||||||
25989|Lavery Creek Granite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Probable Early to Middle Ordovician||||||15-JUL-14
25989|Lavery Creek Granite|43259|4|Described|Appendix 1,p21.||Ordovician|||||||
25989|Lavery Creek Granite|43933|5|Briefly described|Map Legend||Ordovician|||||||
25989|Lavery Creek Granite|43934|5|Briefly described|Map Legend||Ordovician|||||||
25989|Lavery Creek Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
25989|Lavery Creek Granite|62521|5|Briefly described|p9, p26|Middle Ordovician|Late Cambrian|Of the Lavery Creek Supersuite. Geological Province: Ravenswood Batholith. Intruded by Chipley Granite. Comprises mainly quartz, potash feldspar, plagioclase and biotite.||||||14-JAN-08
25989|Lavery Creek Granite|68576|6|Mentioned|Q_11: p42|||Charters Towers.||||||
25989|Lavery Creek Granite|68731|6|Mentioned|p149|||Mafic pillows are common in parts of the Lavery Creek Granite.||||||
73534|Lavery Creek Suite|62521|5|Briefly described|p30|||Of Lavery Creek Supersuite. Comprises all the supersuite granites except Fenian Granite of the Fenian Suite; includes Lavery Creek and Mount Boddington Granites, Piano Gully Granodiorite and Carlyon Creek Complex granites. Geol.Prov: Ravenswood Batholith.||||||14-JAN-08
73534|Lavery Creek Suite|68731|6|Mentioned|p149|||||||||
34661|Lavery Creek Supersuite|22847|6|Mentioned|p 10|||||||||
34661|Lavery Creek Supersuite|23422|4|Described|p172, p209 Table 6.6|Middle Ordovician|Middle Ordovician|||||||
34661|Lavery Creek Supersuite|23430|5|Briefly described|p481|||Ravenswood Batholith Province.||||||
34661|Lavery Creek Supersuite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
34661|Lavery Creek Supersuite|23893|5|Briefly described|p12|Middle Ordovician|Late Cambrian|Geological Province: Macrossan Province.||||||
34661|Lavery Creek Supersuite|62521|4|Described|p30|Middle Ordovician|Early Ordovician|Comprises 2 suites: main Lavery Creek Suite and Fenian Suite which together include: Lavery Creek, Mount Boddington and Fenian Granites, Piano Gully Granodiorite and Carlyon Creek Complex granites. Geol.prov: Ravenswood Batholith. See also p1, p26.||||||21-DEC-07
34661|Lavery Creek Supersuite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Chipley, Columbia Creek (part), Hogsflesh and Brittany Supersuites; Schreibers and Sunburst Suites; the Lynwater Complex; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
34661|Lavery Creek Supersuite|68731|6|Mentioned|p148, p149, p150|Middle Ordovician|Early Ordovician|Hutton and Crouch (1993); Hutton et al. (1994); Hutton and Rienks (1997).|||||Comprises mainly pink to red and grey biotite and hornblende-biotite granitoids.|15-JUL-14
40579|Lawn Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Amos Formation, Smythe Sandstone and lower parts of Balbirini Dolostone.|||
40579|Lawn Supersequence|63866|5|Briefly described|p53|||Isa Superbasin.|||Includes the Amos Formation and the Balbirini Dolomite, lower.|||
40579|Lawn Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Statherian|Statherian|Lawn Hill Platform and southern McArthur River Region. SHRIMP zircon ages from tuffs. Base is at the base of the Amos Formation, not above it (as in previous studies).|1616 +/- 5 Ma and 1611 +/- 4 Ma.|||Is overlain by Wide Supersequence.|Tuffaceous sandstones and carbonaceous shales.|
40579|Lawn Supersequence|66843|5|Briefly described|p36-39|||Said to be "informally" named, after the Lawn Hill Formation, because unit Pmh4 in the middle part of the Formation contains the MFS of this basin phase. Depositional cycles and lithofacies detailed.|~1615 - 1595 Ma.|||||
40579|Lawn Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40579|Lawn Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Camooweal - Murphy Domain, Mount Isa Inlier. Also recognised within the Nathan Group, NT. ||||Overlies Term Supersequence. Is overlain by Wide Supersequence.|Grey to black carbonaceous shale and siltstone, greenish grey tuff and tuffaceous siltstone, micaceous lithic sandstone and conglomeratic sandstone.|
40579|Lawn Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation.||||||
40579|Lawn Supersequence|69056|6|Mentioned|p56|||||||||
40579|Lawn Supersequence|69591|5|Briefly described|p27, p43, p47, p54|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the lower part of Lawn Hill Formation.||||Is equated with lower part of Doomadgee Formation.||
40579|Lawn Supersequence|70897|5|Briefly described|p39, Fig.1.7.1-3,7|Mesoproterozoic|Mesoproterozoic|Maintains relatively tabular architecture throughout deposition.||||Overlies Term Supersequence. Is overlain by Wide Supersequence.||
40579|Lawn Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic| Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation.|||||Grey to black carbonaceous shale and siltstone, greenish grey tuff and tuffaceous siltstone, micaceous lithic sandstone and conglomeratic sandstone.|
40579|Lawn Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||||
40579|Lawn Supersequence|72912|5|Briefly described|p33, p35 Fig.13, p45-46.|Paleoproterozic|Paleoproterozic|||||Overlies Term Supersequence and underlies Wide Supersequence.||
40579|Lawn Supersequence|73144|4|Described|p4-5, p8-9, p12, p20, p25, p40, p45, p49|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains four third order sequences [see article for more detail on third order sequences]. Deposited in inner-mid-outer shelf and possible submarine fan (Krassay et al., 2000). Drilling at Egilabria-4 has confirmed the presence of multiple thick and organic-rich shale gas intervals (Lawn Shale Gas Play). Potential source rock but maturity ranges are over 1.2% EqVR and 2% EqVR at Desert Creek 1 and Egilabria 1 wells respectively. Followed a significant erosional event. Third-order sequence Lawn 4 is considered one of [two] principal source rocks for the Isa Superbasin.|1600-1615 Ma|||Includes a portion of the Lawn Hill Formation.|Sandstone, siltstone, carbonaceous silty shale, silty shale and shale.|
38872|Lawyer Granite|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38872|Lawyer Granite|24615|5|Briefly described|CD|Triassic|Triassic|[Rggl/g].  Pale pink, medium-grained hornblende-biotite granodiorite and granite.||||||
38872|Lawyer Granite|67203|5|Briefly described|p7|Triassic|Triassic|Despite slightly younger K-Ar ages (Webb and McDougall, 1968), intrusive relationships indicate that this unit (and Deception Quartz Monzonite, Rule Gabbro) is marginally older than the Robert Granite (230.2+/-3.7Ma), and therefore broadly contemporaneous with the Bobby Volcanics, Agnes Water Volcanics and other granitoids further east.||Unit in Glassford Igneous Complex.||Intrudes Bobby Volcanics.|Dominantly high-level (miarolitic and granophyric), leucocratic, alkali-rich granites to quartz monzonites and small gabbro bodies.|12-NOV-15
38872|Lawyer Granite|68008|2|Defined|p290, p334, p336, p402-405, p407, p635|Late Triassic|Late Triassic|A zoned pluton in the south of the Igneous Complex was recognised by Crick (1963) and Hill (1963). Here named after Lawyer Creek. The type area is along Little Glassford Creek, from its junction with Coppermine Creek to the western contact of the intrusion at Blue Bag Cu mine. Centred 15km WSW of Many Peaks town; covers about 30 km2. Forms hilly topography. Geophysics described in some detail and modelled. Geochemistry detailed: similar to Littlemore Granodiorite. Garnet and magnetite-rich skarns occur around the intrusion, producing Cu at Blue Bag and Lady Inez deposits; Zn-rich skarns occur at Mount Sperber. This and similar age determinations conflict with the age of the supposedly intrusive Robert Granite of 230.2 +/- 3.7 Ma; discussed.|226 +/- 4.5 Ma (Webb and McDougall, 1968).|Glassford Igneous Complex.||Intrudes Rockhampton Group. Is intruded by Rule Gabbro, Robert Granite and Deception Quartz Monzonite.|The central granite phase is pinkish grey, medium- to coarse-grained, equigranular biotite-hornblende granite. The marginal phase is grey, medium-grained, equigranular augite-hornblende-biotite quartz monzodiorite. Local foliated quartz gabbro.|
38872|Lawyer Granite|68679|5|Briefly described|p427, p431|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Geochemistry briefly described.|226 +/- 4.5 Ma (K-Ar: Webb and McDougall, 1968).|Glassford Igneous Complex.|||Medium-grained, quartz monzodiorite rim, locally foliated, surrounding a central phase of hornblende-biotite granite and granodiorite.|
38872|Lawyer Granite|73450|6|Mentioned|p11, p14|Triassic|Triassic|||||Intruded by Roberts Granite.||
26684|Laytons Range Conglomerate|12597|5|Briefly described|p491, p492 Tb.1|Rhaetian|Rhaetian|S Clarence-Moreton Basin. Basal, high energy fluvial deposits on top of eroded surface of Ipswich and Nymboida Basins. Appears as Laytons Ranges Cgl in Tb.1.||Unit in Bundamba Group.|||Conglomerate, coarse lithic sandstone.|
26684|Laytons Range Conglomerate|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rahetian|Of the Woogaroo Subgroup (Bundamba Group). Polymictic pebble-cobble conglomerate (basal rudite); minor sandstone. Max. thickness: 80m. Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|22865|6|Mentioned|Fig.22.10ap318|||||||||
26684|Laytons Range Conglomerate|23811|5|Briefly described|Map Legend|Rhaetian|Rhaetian|Of Woogaroo Subgroup.  Polymictic pebble and cobble ortho- and paraconglomerate; subordinate lenses/beds of coarse-grained, crossbedded sublithic to lithic sandstone.  Clasts incl. chert, volcanic and sedimentary rock.  Geol:Prov: Clarence-Moreton Basin.||||||20-DEC-04
26684|Laytons Range Conglomerate|23812|5|Briefly described|p35 Tb.4|Late Triassic|Late Triassic|Of Bundamba GRoup.  Maximum thickness: 80m.  Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|30911|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
26684|Laytons Range Conglomerate|31806|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
26684|Laytons Range Conglomerate|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
26684|Laytons Range Conglomerate|33476|4|Described|p102|||Mention p90.||||||22-MAY-08
26684|Laytons Range Conglomerate|33766|6|Mentioned|Map legend|Jurassic|Triassic|Jurassic - Triassic||||||
26684|Laytons Range Conglomerate|34340|3|Fully described|p465|||||||||
26684|Laytons Range Conglomerate|39279|6|Mentioned|Fig. 1|||||||||
26684|Laytons Range Conglomerate|39907|4|Described|p10|||Sedimentology||||||
26684|Laytons Range Conglomerate|41631|6|Mentioned|p9|||||||||
26684|Laytons Range Conglomerate|42248|6|Mentioned|p408|||||||||
26684|Laytons Range Conglomerate|42463|6|Mentioned|Fig.3 P170|||||||||
26684|Laytons Range Conglomerate|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
26684|Laytons Range Conglomerate|43736|5|Briefly described|Table 1,p4|||||||||
26684|Laytons Range Conglomerate|44450|5|Briefly described|p9|Late Triassic|Late Triassic|Geological Province: New England Fold Belt.||||||
26684|Laytons Range Conglomerate|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Conglomerate and sandstone.||||||
26684|Laytons Range Conglomerate|60281|5|Briefly described|p30, Fig. 18 App 1|Late Triassic|Late Triassic|See also the informal Laytons Range conglomerate.  Of the Woogaroo Subgroup (Bundamba Group).  Conglomerate, minor sandstone.  Overlain by Raceview Formation. Max. thickness: 80m.  Geological Province: Clarence-Moreton Basin.||||||17-MAR-05
26684|Laytons Range Conglomerate|60993|5|Briefly described|p6|Late Triassic|Late Triassic|Of the Woogaroo Subgp. Previously mapped as Corindi Conglom., but this name now discarded. Incorporates the Aberdare Conglom. Pebble to boulder conglomerate; minor shale, siltstone, coal. Geol. Prov: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|60995|4|Described|p55-56, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp; equivalent of Aberdare Conglom. Pebble and cobble conglomerate, minor sandstone. Overlain by Raceview Fm or Gatton Sst.  Max. thickness: 80m. Geol. Prov: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|60996|5|Briefly described|p72|||Grades up into Raceview Formation and also unconformably overlain by Gatton Sandstone; near Baryulgil, overlain conformably by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin. Equivalent of Aberdare Conglomerate.||||||
26684|Laytons Range Conglomerate|60997|5|Briefly described|p140|||Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
26684|Laytons Range Conglomerate|60999|5|Briefly described|p164|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6.||||||
26684|Laytons Range Conglomerate|61004|5|Briefly described|p232 Fig. 2|Triassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
26684|Laytons Range Conglomerate|61006|5|Briefly described|p279 Tb. 1|Triassic|Triassic|Conglomerate, labile sandstone, mudstone. See also p279 Tb. 1.||||||
26684|Laytons Range Conglomerate|61310|5|Briefly described|p21, Table C1 (p22-23)|Late Triassic||Of the Woogaroo Subgroup. Pebble/cobble conglomerate, minor sandstone. Geological Province: Clarence-Moreton Basin||||||
26684|Laytons Range Conglomerate|64665|5|Briefly described|p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin. ||||Is overlain by Raceview Formation.|High energy conglomerate and sandstone.|
26684|Laytons Range Conglomerate|67402|5|Briefly described|p165 tbl LPB1, p187, p188, p193|||Clarence-Moreton Basin.||Woogaroo Subgroup|||Conglomerates with minor coarse lithic sandstones.|
26684|Laytons Range Conglomerate|69297|5|Briefly described|p487 fig 5.38|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. More than 50m thick. ||Woogaroo Subgroup||Overlies the Redcliff Coal Measures. Overlain by the Raceview Formation.||
26684|Laytons Range Conglomerate|69594|5|Briefly described|p543-544|||Clarence-Moreton Basin (NSW). Is known as Aberdare Conglomerate in QLD. The basal shale-siltstone is <1m thick and consists of weathered needles of iron carbonate in a pinkish Fe-rich matrix; it forms a consistent marker bed in many boreholes.||Woogaroo Subgroup.||Is overlain by Raceview Formation.|Pebble to cobble conglomerate; some beds with rippled fine sandstone laminae, others extensively rooted, thin claystones in places; a pinkish grey shale and siltstone underlies conglomerate at base.|
26684|Laytons Range Conglomerate|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
26684|Laytons Range Conglomerate|71628|5|Briefly described|p9: 5, 11, 32; p19: 24, 147|Triassic|Triassic|Clarence-Moreton Basin.||Woogaroo Subgroup.||Overlies Purgatory Monzogranite, Bruxner and ?Cullens Creek Granodiorites and (locally) Dumbudgery Creek Complex and Jenny Lind Tonalite.||
26684|Laytons Range Conglomerate|73570|5|Briefly described|p911, p912 Fig.2, p913-915, p919-920|Rhaetian|Norian|Clarence-Moreton Basin, lower part. Paleocurrent directions are generally radial into the basin. Very local provenance from New England Orogen. Abbreviated as Laytons Conglomerate p917 Fig.5.||||Overlies Ipswich Coal Measures, underlies Raceview Formation||
25158|Leander Quartzite|23031|6|Mentioned|47 fig 11|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25158|Leander Quartzite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
25158|Leander Quartzite|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
25158|Leander Quartzite|24033|5|Briefly described|p5|||Includes orthoquartzite, feldspathic quartzite, micaceous metasiltstone, phyllite and tuff.||||||
25158|Leander Quartzite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group.  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
25158|Leander Quartzite|29961|6|Mentioned|p6|||||||||
25158|Leander Quartzite|29966|6|Mentioned|p396|||||||||
25158|Leander Quartzite|30534|3|Fully described|p300|||||||||
25158|Leander Quartzite|32660|5|Briefly described|Table 5|||||||||
25158|Leander Quartzite|32959|6|Mentioned|Fig.21|||||||||
25158|Leander Quartzite|33900|5|Briefly described|p13|||Mention p10.||||||15-MAR-07
25158|Leander Quartzite|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25158|Leander Quartzite|35074|6|Mentioned|Fig.2|||||||||
25158|Leander Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25158|Leander Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25158|Leander Quartzite|37459|6|Mentioned|p427|||||||||
25158|Leander Quartzite|37568|5|Briefly described|p81|||||||||
25158|Leander Quartzite|38232|6|Mentioned|p83|||See also p87.||||||15-MAR-07
25158|Leander Quartzite|38560|6|Mentioned|p114|||||||||
25158|Leander Quartzite|38919|6|Mentioned|p496|||||||||
25158|Leander Quartzite|39445|5|Briefly described|Table 2|||See also p40.||||||15-MAR-07
25158|Leander Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25158|Leander Quartzite|39934|6|Mentioned|Fig.3|||||||||
25158|Leander Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25158|Leander Quartzite|40221|3|Fully described|p6|||||||||
25158|Leander Quartzite|40840|6|Mentioned|Map legend|||||||||
25158|Leander Quartzite|41125|6|Mentioned|p48|||||||||
25158|Leander Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
25158|Leander Quartzite|41978|6|Mentioned|p501|||||||||
25158|Leander Quartzite|42565|5|Briefly described|Table 1 P5|||||||||
25158|Leander Quartzite|44210|2|Defined|map,Tb.1,p8,10,11|||||||||
25158|Leander Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
25158|Leander Quartzite|44271|2|Defined|p33,37,53|||||||||
25158|Leander Quartzite|44275|14|Not recorded|Map Legend|||||||||
25158|Leander Quartzite|44276|14|Not recorded|Tb.1|||||||||
25158|Leander Quartzite|44278|2|Defined|Tb.1,map,p7|||||||||
25158|Leander Quartzite|44521|14|Not recorded|p24,map|||||||||
25158|Leander Quartzite|44755|14|Not recorded|Fig.1,p93||Mesoproterozoic|||||||
25158|Leander Quartzite|44765|14|Not recorded|p15,16||Paleoproterozoic|||||||07-NOV-08
25158|Leander Quartzite|44989|2|Defined|p.64-5|||Tb.III. On many pages. Underlies Eastern Creek Volcanics. (F54-1,2).||||||
25158|Leander Quartzite|45166|4|Described|p14|||||||||
25158|Leander Quartzite|45287|14|Not recorded|p.225,226|||Contemp.with Mount Guide and Ballara Quartzite.||||||15-MAR-07
25158|Leander Quartzite|47083|5|Briefly described|p6|||||||||
25158|Leander Quartzite|50100|5|Briefly described|p16-17|Statherian|Statherian|Of Lower Haslingden Group. Conformably overlain by Eastern Creek Volcanics. Geological Province: Western Fold Belt. Lower: greywacke, schist,phyllite feldspathic sst., basalt, tuff+pyritic sltst; upper: qtz sst., feldspathic sst. and quartzite +arkose,con||||||15-MAR-07
25158|Leander Quartzite|50332|5|Briefly described|p17|Proterozoic|Proterozoic|Of the lower Haslingden Group. Overlain comformably by Myally Subgroup.||||||07-FEB-11
25158|Leander Quartzite|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin. Shown as Leander Qzit.||||||
25158|Leander Quartzite|66529|6|Mentioned|p34|||||||||
25158|Leander Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p31|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Leichhardt Superbasin. Marine facies.|~1780 Ma.|Lower Haslingden Group.|||Orthoquartzite, feldspathic quartzite; schist, arkose, metabasalt.|
25158|Leander Quartzite|69591|5|Briefly described|p33, p57, p105|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Guide Supersequence.||Haslingden Group.||Equated with Mount Guide Quartzite.|Orthoquartzite, feldspathic quartzite; schist, arkose, metabasalt.|
25158|Leander Quartzite|71960|5|Briefly described|p85-86, p77, p80, 82,  p83 Fig.6, |Proterozoic|Proterozoic|In ?tectonic contact with Eastern Creek Volcanics in Leander Anticline.||Of Haslingden Group.||||
25158|Leander Quartzite|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|Coastal, shelf environment.||Of Haslingden Group|||Arkose, feldspathic sandstone.|
25158|Leander Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Siliciclastics.|
23720|Leconsfield Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23720|Leconsfield Granite|22781|4|Described|p33|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
23720|Leconsfield Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Barwon Granite and Burns Granite||||||
23720|Leconsfield Granite|42610|2|Defined|p10|Early Devonian|Early Devonian|This unit was included in the "Kintore Adamellite" of B135.||||||
23720|Leconsfield Granite|43738|6|Mentioned|Fig.12,p38|||||||||
23720|Leconsfield Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
82986|Leichhardt Creek Basalt|73115|6|Mentioned|p29|Pleistocene|Pleistocene|McBride Basalt Province.|0.26-0.3 Ma|||||
75760|Leichhardt Range Granite|69593|5|Briefly described|p494 Fig.6.15, p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|290 Ma.||||I-type.|
75760|Leichhardt Range Granite|70740|5|Briefly described|p124, p126|||Distribution is briefly discussed.|||||Mainly medium-grained, slightly uneven-grained to moderately porphyritic leucocratic muscovite-biotite and biotite monzogranite to syenogranite. Minor biotite monzogranite and rare tourmaline syenogranite.|
38247|Leichhardt Suite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Supersuite.||||||
38247|Leichhardt Suite|69593|4|Described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|Barratta, Drynoch, Miners Gap, Molybdenite Creek Granites; Lulu Pocket, Mount Canton, Igneous Complexes; Marlborough Pocket Granodiorite.||Biotite and hornblende-biotite granodiorite, granite and microgranite; also dacite, dacitic tuff, rhyolite.|
34680|Leichhardt Supersuite|22847|5|Briefly described|p 15|||||||||
34680|Leichhardt Supersuite|23422|4|Described|p184, p218 table 6.12|Early Permian|Late Carboniferous|||||||
34680|Leichhardt Supersuite|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Charters Towers Province.||||||
34680|Leichhardt Supersuite|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as the Badu Suite and parts of the Almaden, Ingham, O'Briens Creek and Ootann Supersuites, and various ungrouped Carboniferous-Early Permian plutonic units, are all mapped under the symbol, CPgk.||||||
34680|Leichhardt Supersuite|68900|6|Mentioned|p4|Early Permian|Carboniferous|Drummond Basin.||||||
34680|Leichhardt Supersuite|69593|4|Described|p491-496, p504|Permian|Late Carboniferous|Rienks et al. (1995). Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. Commonly associated with extrusives of the Camp Oven Mountain Complex, Mount Canton Igneous Complex, and Black Pinnacle Igneous Complex.|~310-283 Ma.||Tuckers, Leichhardt, Bogie Suites; Pall Mall, Mingoom, Speed Creek Granites; Emysland Granodiorite.||Mostly relatively felsic: biotite and hornblende-biotite granodiorite, granite and microgranite as well as hypabyssal equivalents (dacite and rhyolite); also gabbro to granite complexes. I-type.|
34680|Leichhardt Supersuite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||Includes Tuckers Suite.|||
28675|Leichhardt Volcanics|22665|6|Mentioned|P220||Orosirian|||||||
28675|Leichhardt Volcanics|22680|6|Mentioned|83|Proterozoic|Proterozoic|||||||
28675|Leichhardt Volcanics|23333|6|Mentioned|1113|||||||||
28675|Leichhardt Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
28675|Leichhardt Volcanics|23518|4|Described|p10|Proterozoic|Proterozoic|Of Tewinga Group.  Geological Province: Kalkadoon-Ewen Province.||||||
28675|Leichhardt Volcanics|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28675|Leichhardt Volcanics|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28675|Leichhardt Volcanics|37862|4|Described|p581|||||||||
28675|Leichhardt Volcanics|38234|4|Described|p100|||||||||
28675|Leichhardt Volcanics|38235|6|Mentioned|p115|||||||||
28675|Leichhardt Volcanics|38350|4|Described|p6|||||||||
28675|Leichhardt Volcanics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28675|Leichhardt Volcanics|38900|6|Mentioned|p53|||||||||
28675|Leichhardt Volcanics|40623|5|Briefly described|p97|||||||||
28675|Leichhardt Volcanics|40840|6|Mentioned|Map legend|||||||||
28675|Leichhardt Volcanics|40984|4|Described|p389|||||||||
28675|Leichhardt Volcanics|41325|6|Mentioned|p18|||||||||
28675|Leichhardt Volcanics|41381|6|Mentioned|p323|||||||||
28675|Leichhardt Volcanics|41744|6|Mentioned|p406|||||||||
28675|Leichhardt Volcanics|41791|6|Mentioned|p266|||||||||
28675|Leichhardt Volcanics|41961|6|Mentioned|p38|||||||||
28675|Leichhardt Volcanics|41970|6|Mentioned|p332|||||||||
28675|Leichhardt Volcanics|41978|5|Briefly described|p497|||See also p494.||||||15-MAR-07
28675|Leichhardt Volcanics|41979|6|Mentioned|Table 1 P510|||||||||
28675|Leichhardt Volcanics|42565|4|Described|Table 1 P6|||||||||
28675|Leichhardt Volcanics|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1865Ma. Porphyritic felsic volcanics.||||||09-FEB-09
28675|Leichhardt Volcanics|43608|6|Mentioned|Fig.11,p11|||||||||
28675|Leichhardt Volcanics|43616|6|Mentioned|p2|||1860 Ma||||||
28675|Leichhardt Volcanics|43928|6|Mentioned|23|||||||||
28675|Leichhardt Volcanics|44195|6|Mentioned|p356 Fig.9|||||||||
28675|Leichhardt Volcanics|45161|4|Described|p18|||See also Table 5||||||
28675|Leichhardt Volcanics|45166|4|Described|p11|||||||||
28675|Leichhardt Volcanics|45167|5|Briefly described|p50|||||||||
28675|Leichhardt Volcanics|49009|2|Defined|p21|Paleoproterozoic|Paleoproterozoic|Mapped as Leichhardt Metamorphics by Carter & Opik (1963).||||||07-NOV-08
28675|Leichhardt Volcanics|49041|6|Mentioned|Table 4|||||||||
28675|Leichhardt Volcanics|50100|5|Briefly described|p11, p13 Fig. 4|Orosirian|Orosirian|Mainly felsic ignimbrites.  Unconformably overlain by Magna Lynn Metabasalt, Argylla Formation, Eastern Creek Volcanics, Myally Subgroup and Quilalar Formation.  Also overlain by Makbat Sandstone.  Intruded by Kalkadoon Granodiorite.||||||
28675|Leichhardt Volcanics|50332|5|Briefly described|p10, p16-17, p20, p50, p66|Proterozoic|Proterozoic|Unconformably overlain by Magna Lynn Metabasalt, Argylla Formation, Eastern Creek Volcanics, Myally Subgroup, Quilalar Formation, Surprise Creek Group. Consist mainly of felsic ignimbritic deposits + lava flows, dacitic to rhyolitic in composition.||||||07-FEB-11
28675|Leichhardt Volcanics|50536|5|Briefly described|p1.4, 2.1, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite. Age: 1886-1852 +/- 32Ma (U-Pb, Shrimp). Intruded by Wonga Suite.||||||07-NOV-08
28675|Leichhardt Volcanics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Porphyritic felsic volcanics. Of the Tewinga Group.||||||
28675|Leichhardt Volcanics|60558|5|Briefly described|p4 Fig. 3, p9 Fig. 7|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block and Western Fold Belt.||||||03-JUN-09
28675|Leichhardt Volcanics|61922|5|Briefly described|p8, p9 Fig. 3|Paleoproterozoic|Paleoproterozoic|Comprise dacitic to rhyolitic ignimbrite flows. Age: ~1860Ma. Geological Province: Mount Isa Inlier. See also p17-18 Figs.9 and 10.||||||07-NOV-08
28675|Leichhardt Volcanics|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1866+/-5Ma. See also p145.||||||07-NOV-08
28675|Leichhardt Volcanics|61933|6|Mentioned|p177|||Dominated by felsic lavas and contain only rare mafic lavas and psammite; variably weakly foliated to schistose.||||||
28675|Leichhardt Volcanics|61936|5|Briefly described|p195 Fig. 6|||Geological Province: Kalkadoon/Leichhardt Fold Belt, Mount Isa Inlier. ||||||
28675|Leichhardt Volcanics|63866|5|Briefly described|p59|||Kalkadoon-Leichhardt Belt. According to the authors this unit is also referred to as the Leichhardt Metamorphics.||||||
28675|Leichhardt Volcanics|64248|6|Mentioned|p32, p38 Fig.5|Orosirian|Orosirian|The first cover sequence in this study of the Eastern Succession. Appears as Leichhardt volcanics on p32.|1875 +/- 23 to 1852 +/- 7 Ma.|||Overlies Plum Mountain Gneiss.||11-DEC-17
28675|Leichhardt Volcanics|64250|5|Briefly described|p11 fig 3, p27, p19|||Kalkadoon-Leichhardt Belt, Mount Isa Inlier.Co-magmatic with Kalkadoon Granite. Hosts the Mount Cuthbert Cu+/-Au deposit.|1875 +/- 23 Ma to 1852 +/- 7 Ma.||||Includes minor metabasalt; rare sedimentary units.|14-MAR-18
28675|Leichhardt Volcanics|64254|5|Briefly described|p161, p162|Paleoproterozoic|Paleoproterozoic|Age: 1860Ma (SHRIMP). Geological Province: Kalkadoon - Leichhardt Belt.||||||
28675|Leichhardt Volcanics|64567|5|Briefly described|p1095-1098|Paleoproterozoic|Paleoproterozoic|SHRIMP U/Pb zircon age 1867 +/- 5 Ma. Comagmatic felsic volcanics.||||||
28675|Leichhardt Volcanics|64722|5|Briefly described|Fig. 2 p3-6, p11, 27|Orosirian|Orosirian|Mount Isa region. Felsic in composition. Geochemical data suggest a magmatic arc depositional setting.|1875 - 1845 Ma.|||||11-APR-12
28675|Leichhardt Volcanics|65228|6|Mentioned|p20.|||Formerly Leichhardt Metamorphics. Low grade metamorphosed. May possibly correlate with the Scrutton and Cliffdale Volcanics.||||||
28675|Leichhardt Volcanics|65387|4|Described|p1, p3 Tb.1, p76-81|Orosirian|Orosirian|Kalkadoon-Leichhardt Belt. Magmatic crystallisation age. Also referred to informally as the Leichhardt suite. These Volcanics have been associated with the Kalkadoon Granite (emplaced c.1862 to 1847 Ma).|1864 +/- 3 Ma SHRIMP zircon (Carson et al. 2008).|||Is overlain disconformably by Magna Lynn Metabasalt.|Mainly rhyolitic to dacitic ignimbrite and minor flow-banded lava; dominant lithology is grey, weakly magnetic quartz-feldspar porphyry; includes foliated rhyodacite.|
28675|Leichhardt Volcanics|65396|5|Briefly described|p4, p7, p17, p80, p82, p84, p86, p90|Orosirian|Orosirian|See also p175, p186, p192, p201, p241, p437. Eastern succession, Cover Sequence 1. Kalkadoon-Leichhardt Belt. Co-genetic with Kalkadoon Granite. Hosts the Mount Cuthbert Cu+/-Au deposit.|1875 +/- 23 Ma - 1852 +/- 7 Ma||||Voluminous felsic volcanics; rare sedimentary units and minor metabasalt.|04-APR-17
28675|Leichhardt Volcanics|65505|5|Briefly described|969, 978, 981, Fig1-4|Proterozoic|Proterozoic|Kalkadoon-Leichhardt Block basement, Age: 1860 +/- 3Ma (zircon). Grey banded gneiss, with sedimentary and granitic clasts.||||||
28675|Leichhardt Volcanics|66882|6|Mentioned|p117|||Discussed but rejected as possible source for felsic juvenile material in Cleve Group.||In Kalkadoon Suite.||||
28675|Leichhardt Volcanics|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
28675|Leichhardt Volcanics|67323|4|Described|p9, p14-15, p23, p29, p39-40, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Post-Barramundi basement. Western Mary Kathleen Domain, Kalkadoon-Leichhardt Domain, central Mount Isa Block. Possible arc formed during W-dipping subduction.|1865 +/- 3 Ma; 1852 +/- 7 Ma.||Includes Candover beds, Orient beds,|Is intruded by Ewen Granite. Correlated with Cliffdale Volcanics.|Massive to schistose, felsic metavolcanics, commonly porphyritic with quartz and feldspar phenocrysts; minor breccia, bedded meta-tuff, meta-sandstone, sericitic schist, phyllite.|
28675|Leichhardt Volcanics|67497|5|Briefly described|p887|Orosirian|Orosirian||1870-1850 Ma (Page 1983) |||Comagmatic with the Kalkadoon Granite.||
28675|Leichhardt Volcanics|67539|5|Briefly described|p10, p11|||Contains belts of less potassic rocks, which appear as dark greenish on composite radiometric images. Variably low to moderately magnetic.||||Overlain by the Magna Lynn Metabasalt.|Felsic volcanics mainly ignimbrite, but locally some rhyolitic flows.|
28675|Leichhardt Volcanics|68146|5|Briefly described|p70, p193|||Part of the crystalline basement of the Kalkadoon-Leichhardt Domain.|c.1860 Ma; Page (1978) and others.|||||
28675|Leichhardt Volcanics|68307|5|Briefly described|p78, p94|Paleoproterozoic|Paleoproterozoic|North Australian Craton. Part of the basement of the Mount Isa Province. Has strong magmatic arc-like geochemical signature. Grouped with the Kalkadoon Granodiorite as a "magmatic suite".|c.1875-1850 Ma.|||||
28675|Leichhardt Volcanics|68542|5|Briefly described|p12|Paleoproterozoic|Paleoproterozoic||1860 Ma||||ashflow tuffs, felsic to dacitic volcanics.|
28675|Leichhardt Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
28675|Leichhardt Volcanics|68575|5|Briefly described|p1, p75, p124|||Kalkadoon-Leichhardt Domain, Mount Isa Province.|c.1860 Ma (Page, 1978).|||||
28675|Leichhardt Volcanics|68576|5|Briefly described|Q_2: p12|||Comagmatic with Kalkadoon Granite. Same age as Whitewater Volcanics in the Kimberley region; possibly part of a vast array of coalescing caldera fields across northern Australia.|1860 Ma.||||Felsic to dacitic volcanics: includes ashflow crystal tuffs.|
28675|Leichhardt Volcanics|69056|4|Described|p2-5, p13, p18, p23, p28, p52|Orosirian|Orosirian|See also Time-Space plot sheet. Basement to the Mary Kathleen and Constantine Domains. Largely unexposed. Modelling values listed. Broadly coeval with Kalkadoon Granodiorite.|1864 +/- 3 Ma (Magee et al., 2012).|||Is overlain by Boomarra Metamorphics and Argylla Formation. Intruded by Kalkadoon Granodiorite.|Felsic volcanic-dominated: typically a sequence of grey quartz feldspar porphyry.|
28675|Leichhardt Volcanics|69222|5|Briefly described|p222 Fig.2|||Kalkadoon-Leichhardt Fold Belt.|1866 +/- 5 Ma|||Intruded by Big Toby granite||09-FEB-18
28675|Leichhardt Volcanics|69591|4|Described|p29-32, p34, p53, p58|Paleoproterozoic|Paleoproterozoic|Basement rocks in Kalkadoon-Leichhardt Domain, Mount Isa Province. Subaerial to subaqueous environment. Is cut by a deformed and metamorphosed basalt dyke dated at 763 +/- 85 Ma (Bierlein et al., 2008), suggesting a post-Isan tectonothermal event in this Domain. Is also intruded by the Ewan Batholith. Ages by Magee et al. (in press) and Wyborn and Page (1983) respectively.|1864 +/- 3 Ma; 1852 +/- 7 Ma.|||Is intruded by Kalkadoon Granodiorite.|Mainly grey, non-magnetic, quartz-feldspar-phyric rhyolite (locally preserving volcaniclastic textures); minor breccia, bedded metatuff, metasandstone, sericitic schist, phyllite. Not highly magnetic.|
28675|Leichhardt Volcanics|70282|5|Briefly described|p544 table 1|||Cover sequence 1, Mount Isa. Related to the Barramundi orogeny.|1870-1850 Ma||||Felsic.|13-FEB-18
28675|Leichhardt Volcanics|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Massive to schistose, felsic volcanics, commonly porphyritic with quartz and feldspar phenocrysts; minor breccia, bedded mica-tuff, meta-sandstone, sericitic schist, phyllite.|
28675|Leichhardt Volcanics|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Massive to schistose, felsic volcanics, commonly porphyritic with quartz and feldspar phenocrysts; minor breccia, bedded mica-tuff, meta-sandstone, sericitic schist, phyllite.|
28675|Leichhardt Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1864+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyodacite.|
28675|Leichhardt Volcanics|71799|5|Briefly described|p150 fig 2, p151 fig 3||||||||Silicic volcanics, porphyry.|
28675|Leichhardt Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Orosirian|Orosirian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. U-Pb SHRIMP crystallisation ages given are 1852 +/- 7 Ma, 1857 +/- 20 Ma, 1865 +/- 3 Ma and 1866 +/- 5 Ma.|1866 +/- 5 Ma to 1852 +/- 7 Ma|||Shown as underlying Kalkadoon Granite.||
28675|Leichhardt Volcanics|72596|6|Mentioned|p4, p49, p54|||Kalkadoon-Leichhardt Domain. Along with Kalkadoon Granodiorite, considered the oldest units in the domain.||||Intruded by Bowlers Hole Granite.|Includes felsic rocks.|
28675|Leichhardt Volcanics|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Mary Kathleen Domain and Kalkadoon-Leichhardt Domain.||||Shown as older than Mayfield Gneiss, Woonigan Granite and Kalkadoon Granodiorite.|Porphyritic rhyolite, rhyodacite and dacite, felsic gneiss; minor siltstone and quartzite.|
28675|Leichhardt Volcanics|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Mary Kathleen Domain and Kalkadoon-Leichhardt Domain.||||Shown as older than Mayfield Gneiss, Woonigan Granite and Kalkadoon Granodiorite.|Porphyritic rhyolite, rhyodacite and dacite, felsic gneiss; minor siltstone and quartzite.|
28675|Leichhardt Volcanics|72799|6|Mentioned|p4|||||||||
28675|Leichhardt Volcanics|72889|5|Briefly described|p6 Fig.i, p14, p17, p18 Tb.1.2.|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain. Previous age determinations: 1857+/-20 Ma, 1864+/-3 Ma, 1860.3+/-3.2 Ma (Neumann and Fraser, 2007; Carson et al., 2008; Neumann et al., 2009). Intruded by dolerite dated as 1853+/- 2.9 Ma. Contemporaneous with the Kalkadoon Suite.|c. 1865-1855 Ma.|||Laterally equaivalent to the Soldiers Cap Group. Intruded by dolerite.||25-NOV-20
28675|Leichhardt Volcanics|72912|5|Briefly described|p5 Fig.3.|Orosirian|Orosirian|Located in the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Four U-Pb zircon igneous crystallisation age determinations shown.|1866 +/- 5 Ma to 1852 +/- 7 Ma|||Shown as underlying Kalkadoon Granite.||
28675|Leichhardt Volcanics|73042|6|Mentioned|p4|Orosirian|Orosirian|Mount Isa Province. Geochronology is a suite of U-Pb zircon igneous crystallisation ages including: 1852 +/- 7 Ma, 1857 +/- 20 Ma, 1865 +/- 3 Ma, 1866 +/- 5 Ma.|1852 to 1866 Ma (see comments and Fig.1.2)|||||
28675|Leichhardt Volcanics|73083|6|Mentioned|p53|||||||||
28675|Leichhardt Volcanics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
28675|Leichhardt Volcanics|73413|6|Mentioned|p3, p6, p21, p23, App.1|Orosirian|Orosirian|Mount Isa Inlier, Kalkadoon-Leichhardt Belt. U-Pb TIMS ages of 1865 +/- 3 Ma, 1865 +/- 3 Ma and 1865 +/- 3 Ma reported by Page (1978).|1865-1845 Ma|||Intruded by Kalkadoon Granodiorite.||
28675|Leichhardt Volcanics|73525|5|Briefly described|p4, p19 Fig.13|Orosirian|Orosirian|Leichhardt River, Kalkadoon-Leichhardt, Mary Kathleen, and Mitakoodi-Tommy Creek Domains. See also Leichhardt Volcanic Group.|1854+/-3 Ma, 1852+/-7 Ma crystallisation ages||||Felsic extrusives.|
28675|Leichhardt Volcanics|73529|6|Mentioned|p2 Fig.1|||Mary Kathleen Domain.||||||
28675|Leichhardt Volcanics|73553|5|Briefly described|p6, p8 Fig.1.2.3, p21-23, p42, p246|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain.|1852+/-7 to 1865+/-3 Ma|||Unconformably underlies Magna Lynn Metabasalt, intruded by Bowlers Hole Granite|Felsic volcanics.|
36499|Leigh Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 141.||||||
80677|Leo Creek Granodiorite|71849|3|Fully described|p8, p16, p79, p102-104, p151, p195|Devonian|Devonian|New name, after Leo Creek. Previously part of Kintore Adamellite of Willmott et al. (1973). Elongate, N-aligned pluton of ~14km2 in central McIlwraith Range, c.30km NE of Coen. Proposed type area is around the abandoned Claudie Lakeland mine at MGA 756519 8479871 - MGA 756617 8479976. Geophysics, lithology briefly described. Cut by several auriferous quartz-filled shear zones. Inferred to pre-date McIlwraith Granite. Not isotopically dated; age between ~415-395 Ma from Pama Igneous Association.||Lankelly Suite.||Interpreted to intrude Coen Metamorphic Group. Interpreted to be intruded by McIlwraith Granite.|Grey, fine- to medium-grained, slightly porphyritic muscovite-biotite granodiorite. Moderately deformed. Deeply weathered. Calc-alkaline to high K calc-alkaline, peraluminous S-type.|
80677|Leo Creek Granodiorite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Lankelly Suite.|||Grey, fine- to medium-grained, slightly porphyritic muscovite-biotite granodiorite; moderately deformed.|
83684|Leo Seam|73305|6|Mentioned|p554 Tb.2, p555 Fig.7, p556 Fig.8, p560|Late Permian|Late Permian|Bowen Basin. Third-order 1.9 to 6.35 m thick coal seam within the Burngrove Formation split from the Libra Seam. Correlated across the basin by association with accessory tuffs. See also p558 Fig.10.||Burngrove Formation|||Coal seam.|
74541|Les Jumelles beds|64851|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Very fine- to medium-grained, medium to very thick-bedded quartzose to feldspathic sandstone with local dissolution cleavage; cleaved mudstone or phyllite, locally with abundant spots of retrogressed andalusite.||||||
74541|Les Jumelles beds|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Very fine to medium-grained, medium to very thick-bedded, quartzose to feldspathic sandstone with local dissolution cleavage; cleaved mudstone or phyllite, locally with abundant spots of retrogressed andalusite.||||||10-FEB-09
74541|Les Jumelles beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Ordovician|Cambrian|Mount Windsor Subprovince. This unit, as well as Kirk River beds and Seventy Mile Range Group, are all mapped under the symbol, -COs.||||||
74541|Les Jumelles beds|68679|6|Mentioned|p364|Early Ordovician|Cambrian|Thomson Orogen.||||||
74541|Les Jumelles beds|68731|5|Briefly described|p119 Fig 3.4, p120, p128, p132, p172|Early Ordovician||New unit. Previously mapped as the Anakie Metamorphic Group by Hutton et al. (1998). Includes rocks previously assigned to the Ukalunda beds by Malone et al. (1966). Minimum age constrained by the intrusive Coquelicot Tonalite.|> 471.7 +/- 3.6 Ma|||Unconformably overlain by the Ukalunda Formation, Bimurra Volcanics, Mount Wyatt Formation, and Saint Anns Formation. Intruded by the Coquelicot Tonalite.|Comprises greyish, very fine-grained to medium-grained, medium bedded to very thick bedded, poorly sorted, quartzose to feldspathic sandstone and cleaved mudstone.|11-MAY-16
74541|Les Jumelles beds|68900|2|Defined|p1-p2, p5, p7,  p9, p14-p20|Early Ordovician|Late Cambrian|Outcrops in the south-eastern HARVEST HOME and the north-eastern SCARTWATER. Name is derived from Les Jumelles hill at 513500 7683100. No type sections have been measured however a type area is nominated from 514350 7684000 to 516000 7678650. Previously included within the Ukalunda beds but are now recognised as being too old and thus renamed. Thickness cannot be determined due to complex structure. Petrographic description, structure and distinguishing characteristics are discussed. Intruded by the Coquelicot Tonalite, Percy Douglas Granodiorite, Roscow Granite, Peak John Well Granite and the Joe-de-Little Granodiorite. Faulted against the Anakie Metamorphic Group. See also p26-p30, p50.||Seventy Mile Range Group||Unconformably overlain by the Bimurra Volcanics, Mount Wyatt Formation and the Saint Anns Formation.|Grey to brown, fine- to coarse-grained, medium- to very thick-bedded quartzose meta-arenite and cleaved mudstone or phyllite.|
74541|Les Jumelles beds|68901|6|Mentioned|p2 Fig. i|Early Ordovician|Cambrian|Thomson Orogen.||||||04-OCT-18
74541|Les Jumelles beds|69541|5|Briefly described|p645 Fig.1(b), p654|Cambrian|Cambrian|Thomson Orogen. Middle Cambrian: post-dates the c.500 Ma deformation that is correlated with the Delamerian Orogeny. Potential correlate with Warratta Group.||||Is intruded by the Coquelicot Tonalite.|Sandstone, quartz- to feldspar-rich, poorly sorted, generally massive, interbedded with slate.|
74541|Les Jumelles beds|69952|5|Briefly described|p2 Tb.i, p4, p108-115|Early Ordovician|Cambrian|Anakie Province, Thomson Orogen. Occurs as two NNE-trending parallel belts 60km long and up to 8km wide. Lithologically similar to Puddler Creek Formation. SHRIMP U-Pb zircon maximum depositional age.|528 +/- 9 Ma (Cross et al., 2015).|||Is overlain by Ukalunda Formation. Is intruded by Coquelicot Tonalite. Is faulted against Anakie Metamorphic Group. Correlated with Puddler Creek Formation.|A succession of cleaved sandstone, siltstone and mudstone.|
74541|Les Jumelles beds|70207|6|Mentioned|p1|||Thomson Orogen. Has a detrital age spectrum similar to that of Mount Windsor Volcanics.||||||
74541|Les Jumelles beds|70740|4|Described|i, ii, p1, p2, p8, p9, p12, p14-p20|Ordovician|Ordovician|Drummond Basin, Anakie Inlier. Defined as basement in the Drummond Basin. Name derived from the Les Jumelles Hill.  Appears as Les Jumelles Beds on -1, p2, p8, p126, p129-130. A type area is designated.  Distribution, structure and boundary criteria are discussed. Lithology and petrography are discussed in detail. Thickness cannot be determined. SHRIMP age derived from Cross et al, 2015, Easting and Northing are provided. Intruded by the Coquelicot Tonalite, Joe-de-Little Granodiorite, Percy Douglas Tonalite, Roscow Granite and Peak John Well Granite. See also p22-p24, p28-p30, p32, p33, p34, p47, p72, p80, p126, p130.|476 +/- 6 Ma (SHRIMP U-Pb)|||Unconformably overlain by the Ukalunda Formation. Faulted against the Anakie Metamorphic Group.|Very fine to medium-grained, medium to thickly bedded quartzose to feldspathic sandstone, siltstone and cleaved mudstone.|
74541|Les Jumelles beds|73035|5|Briefly described|Map legend|Ordovician|Cambrian|Informal quartzite subunit recognised.|||||Very fine to medium-grained, medium to very thick-bedded, quartzose to feldspathic sandstone with local dissolution cleavage; cleaved mudstone. Cleaved siltstone and fine-grained quartzite.|
35011|Leura Volcanics|23037|4|Described|p18,9,23-7|Early Permian|Late Carboniferous|Name for diverse assemblage of felsic volcanics. Overlying unit Mount Benmore Volcanics (non-con).||||||28-MAY-08
35011|Leura Volcanics|23042|4|Described|p17,25-9,35,54,68, Fig 2||Carboniferous|Overlying unit Mount Benmore Volcanics, Underlying Unit Connors Volcanics (un).||||||
35011|Leura Volcanics|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPvl].  Trachyandesite to dacite lava, dacitic to rhyolitic ignimbrite and volcaniclastic sediments; locally strongly foliated.||||||
35011|Leura Volcanics|50213|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Overlain by Mount Benmore Volcanics.||||||17-MAY-04
35011|Leura Volcanics|50602|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesitic to dacitic lava, dacitic to rhyolitic ignimbrite and volcaniclastic sediments. Underlies: Mount Benmore Volcanics.||||||30-JUN-04
35011|Leura Volcanics|60445|5|Briefly described|p5, p35, p36|Early Permian|Late Carboniferous|Of Connors Volcanic Group. Felsic to intermediate tuffs and ignimbrites and lavas of trachyandesite to dacite composition, interbedded with thick to medium-bedded sandstone, siltstone and felsic tuff; local conglomerates. Intruded by Waitara Granite.||||||16-MAY-06
35011|Leura Volcanics|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava flows; dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||
35011|Leura Volcanics|60473|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava flows; dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||17-SEP-04
35011|Leura Volcanics|60475|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava, dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||29-SEP-04
35011|Leura Volcanics|60479|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava, dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||
35011|Leura Volcanics|60480|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava, dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||
35011|Leura Volcanics|60481|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Trachyandesite to dacite lava, dacitic to rhyolitic ignimbrite and volcaniclastic sandstone, conglomerate and siltstone; local basal conglomerate.||||||
35011|Leura Volcanics|60557|5|Briefly described|p20 Fig. 5c, p24|Early Permian|Late Carboniferous|Consists of intermediate to felsic lavas and dacitic to rhyolitic ignimbrite, with associated volcaniclastic sediments.||||||09-JUN-05
35011|Leura Volcanics|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35011|Leura Volcanics|61035|5|Briefly described|p7|Early Permian|Late Carboniferous|Of Lizzie Creek Volcanic Group. Age: ~295-299Ma (M. Fanning). Hetrogeneous unit including trachyandesite to dacite lava, sheets of dacite to rhyolitic ignimbrite + volcaniclastic sandstone, conglomerate + siltstone. Geol Prov: Connors Sudprovince.||||||07-FEB-11
35011|Leura Volcanics|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Trachyandesite and dacite lavas, dacitic to rhyolitic ignimbrite and volcaniclastic sst, conglom. and sltst. Basalt to rhyolite flows and volcaniclastics (inc: sst. and conglom. or breccia and felsic ignimbrite). Biotite-pyroxene-hornblende granodiorite.||||||
35011|Leura Volcanics|65388|4|Described|p100-110; p102, 105,  20, 32, 59, 78|Early Permian|Late Carboniferous|Of Connors Volcanic Group, Connors Arch. Relationship and dates suggest unit may be diachronous. Defined: Withnall and others (1998a,b). Overlies Mountain View,  Clive Creek, Broadsound Range, Whelan Creek Volcanics, Bora Creek Quartz Monzodiorite, Tooloombah Granite. Intruded by South Creek Quartz Diorite, Doreen Granite.  Overlain by Tartrus, Cobweb Mountain Rhyolites, Mount Benmore (unconformably), Ametdale and Mount Buffalo Volcanics, Coppermine Andesite, and Back Creek Group. May be equivalent to Glenprarie beds, Camboon Volcanics. SHRIMP ages: 291 +/-3.5 Ma, 307+/-3 Ma, 292+/-4 Ma, 293.5+/-4 Ma. See also p85, 86, 90, 91, 94, 95, 96, 111, 112, 114, 115, 123, 132, 135, 149, 176, 353, 359, 362, 363, 380, 383, 391, 441, 447.||||||
35011|Leura Volcanics|68679|4|Described|p338, p353, p355-362|Cisuralian|Pennsylvanian|Connors Subprovince, New England Orogen. Widely distributed. Total thickness is unknown but >700m. A heterogeneous succession of intermediate to felsic rocks. Source of clasts for Goodedulla beds and Cobweb Mountain Rhyolite's basal conglomerate. This c.291 Ma age is for the northern part of the Subprovince; stratigraphic and intrusive relationships establish a Pennsylvanian age in the south. RELATED UNITS (continued): Overlies Bora Creek Quartz Monzodiorite and Tooloombah Granite nonconformably, the Broadsound Range Volcanics, Burwood Complex and Lotus Creek Rhyolite unconformably, Lotus Creek Rhyolite, and Clive Creek Volcanics (locally). Is thrust against Mount Benmore Volcanics and Back Creek Group. |291 +/- 3.5 Ma (SHRIMP: Fanning et al., 2009).|Connors Volcanic Group.||Is overlain by Tartrus, Cobweb Mountain Rhyolites; Ametdale, Mount Benmore, Mount Buffalo Volcanics; Coppermine, Macksford Andesites. Intruded by South Creek Diorite and Doreen Granite. See COMMENTS.|Crystal-rich volcanilithic sandstone, pebble to boulder conglomerate, dacitic ignimbrite, trachyandesite, rhyolite, rhyolitic ignimbrite, poorly sorted felsic, lithic-rich volcaniclastic rocks.|
35011|Leura Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|294+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite, ignimbrite, rhyolite.|
35011|Leura Volcanics|73197|6|Mentioned|p470-471, p472 Tb.2|Cisuralian|Late Carboniferous|New England Orogen, northern. Northern and eastern margin of the Bowen Basink. Rift volcanic rocks. Grouped with Lizzie Creek Group in U-Pb zircon ages of 283.1 +/- 3.7 Ma and 295.0 +/- 3.4 Ma (Cross et al., 2009; Withnall et al., 2009).|~300-290 Ma||||Volcanics.|
30723|Levian Granite|23396|6|Mentioned|p427|||||||||
30723|Levian Granite|23458|3|Fully described|p119, p129, p115|Mesoproterozoic|Mesoproterozoic|Previously Jessie Granite. Age: 1746+/-8Ma. Part of Naraku Batholith.  3 phases: dominant magnetite-bearing, felsic porphyry, defining crescent-shape of pluton; subordinate phases of fine-grained, grey-pink granite +medium-grained pink-white granite||||||19-DEC-18
30723|Levian Granite|24197|5|Briefly described|p96 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1746Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30723|Levian Granite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
30723|Levian Granite|50332|5|Briefly described|p20|Proterozoic|Proterozoic|Name Levian Granite supersedes Jessie Granite. Of the William and Naraku Batholiths. Age: 1760-1720Ma, (as in the Wonga Suite). Deformed biotite-muscovite pluton.||||||18-APR-12
30723|Levian Granite|50536|5|Briefly described|p1.5, 11.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Levian Suite. Age: 1746 +/- 6Ma (Shrimp).||||||07-NOV-08
30723|Levian Granite|61933|5|Briefly described|p169 Fig.1|||Age: 1740 Ma.||||||15-MAR-07
30723|Levian Granite|63866|5|Briefly described|p61|||||||||
30723|Levian Granite|64248|6|Mentioned|p36, p38 Fig.5|Statherian|Statherian|Southern end of the Naraku Batholith. Same age as Wonga Batholith.|1746 +/- 8 Ma.|||||11-DEC-17
30723|Levian Granite|64250|6|Mentioned|p11 fig 3|||Cloncurry Fold Belt, Mount Isa Inlier.|1746 +/- 8 Ma|||||
30723|Levian Granite|65396|6|Mentioned|p6-7, p40, p53 Fig.1, p82, p84, p90,p175|Statherian|Statherian|See also p218, p241, p361, p439-440, p444-445, p474-500. Eastern succession, Cover Sequence 2. Cloncurry Fold Belt. Stress partitioning and fluid flow models detailed.|1746 +/- 8 Ma|||||
30723|Levian Granite|66913|5|Briefly described|p171 fig 2|Statharian|Statherian|U-Pb zircon SHRIMP age shown diagramatically on Fig. 2.||||||
30723|Levian Granite|67323|4|Described|GIS attrib tbl, p17-18, p24|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Wyborn et al. (2001). Near Cloncurry, Canobie Domain, Mount Isa Inlier. Wonga/Burstall Igneous Event; may be comagmatic with Mount Fort Constantine Volcanics. Deformed during the Isan Orogeny. Similar age to Mount Fort Constantine Volcanics.|1746 +/- 8 Ma (Page and Sun, 1998).|Wonga Suite, Burstall Suite||Intrudes Bulonga Volcanics. Contains enclaves and screens of Mitakoodi Quartzite.|Magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; pink-grey,fine-grained granite; pink-white, medium-grained biotite granite; all phases strongly deformed with local secondary muscovite.|
30723|Levian Granite|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Igneous crystallisation age.|1746 +/- 8 Ma|||||
30723|Levian Granite|69056|4|Described|p14 Tb.3, p18, p23, p28, p53|Statherian|Statherian|See also Time-Space plot sheet. Wonga Event-aged granite to the S of Malakoff Granite, Constantine Domain. Modelling values listed.|1746 +/- 8 Ma (Page and Sun, 1998).|Wonga Suite.||Intrudes Corella Formation.|Strongly deformed, magnetite-bearing felsic porphyry, fine-grained pink-grey granite and a medium-grained biotite granite.|
30723|Levian Granite|69591|5|Briefly described|p36, p60|||Wyborn et al. (2001). Wonga Batholith; Cloncurry area. Similar age to the ~1746-1742 Ma Mount Fort Constantine Volcanics. Similar structural history to Dipvale Granodiorite.|1746 +/- 8 Ma (Page and Sun, 1998).||||Magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; pink-grey, fine-grained granite; pink-white, medium-grained biotite granite; all phases strongly deformed with secondary muscovite.|
30723|Levian Granite|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink-grey, medium-grained biotite granite; magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; all phases commonly strongly deformed with local secondary muscovite.|
30723|Levian Granite|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Pink-grey, medium-grained biotite granite; magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; all phases commonly strongly deformed with local secondary muscovite.|
30723|Levian Granite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink-grey, medium-grained biotite granite; magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; all phases commonly strongly deformed with local secondary muscovite.|
30723|Levian Granite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink-grey, medium-grained biotite granite; magnetite-bearing felsic porphyry with quartz and plagioclase phenocrysts; all phases commonly strongly deformed with local secondary muscovite.|
30723|Levian Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1746+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30723|Levian Granite|72596|6|Mentioned|p24|||Previously[?] Jessie granite.|1746+/-8 Ma|||||
30723|Levian Granite|73553|6|Mentioned|p103, p107|||Previously called Jesse granite.||||||
31458|Lighthouse Suite|23291|5|Briefly described|p33||| Geological Province: Georgetown Region.||||||08-JUL-15
31458|Lighthouse Suite|24197|5|Briefly described|p76, p77|Mesoproterozoic|Mesoproterozoic|Of the Lighthouse Suite. Felsic; veins and pegmatites are common. Age: 1550Ma. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince). See also p79 Tb. 9.1.||||||07-FEB-11
31458|Lighthouse Suite|50537|6|Mentioned|p1.2, 1.5, 5.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Age: 1550Ma||||||19-AUG-04
31458|Lighthouse Suite|69591|5|Briefly described|p80, p82|Mesoproterozoic|Mesoproterozoic|Champion (1991). Eastern margin of the Forsayth Batholith. Age determination by Black and Withnall (1993). Crops out as small irregular bodies.|1561 +/- 10 Ma (U-Pb zircon SHRIMP).||||Migmatitic gneissic granites ranging from homogeneous leucogranite (locally pegmatitic) with almost no biotite, to compositionally banded bodies incorporating biotite-poor and biotite-rich layers.|
37826|Lighthouse Supersuite|23291|4|Described|p33, p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Lighthouse Granite and Lighthouse Suite of Withnall et al 1976. Geochemically different from Forsayth Supersuite.||||||08-JUL-15
37826|Lighthouse Supersuite|63866|5|Briefly described|p76, p78, p86|||Has an affinity with I-type Silurian granites. U-Pb TIMS analyses contain significant portions of inheritance.|||||Irregular-shaped gneissic to pegmatitic, garnetiferous, biotite-muscovite granites.|
37826|Lighthouse Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.|1561 +/- 10 Ma.|||Intrudes Malacura Sandstone.||
37826|Lighthouse Supersuite|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||||
37826|Lighthouse Supersuite|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Etheridge Province. This unit, the Forsayth Supersuite and the Forest Home Supersuite are all mapped under the same symbol, -Pgf.||||||
39883|Lightning Creek Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Creek is Ck in text. Geological Province: Mount Isa Block. Age: ~1519-1509Ma (U-Pb)||||||
39883|Lightning Creek Granite|24257|5|Briefly described|p72 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological Province: Eastern fold belt, Mount Isa Block.||||||
39883|Lightning Creek Granite|60665|6|Mentioned|p1157 Fig.9. |Calymmian|Calymmian|Northern Cloncurry intrusion. Age inferred from Fig.9.|1514 +/- 5 Ma.|||||
39883|Lightning Creek Granite|64250|6|Mentioned|p11 fig 3||||1514 +/-5 Ma; 1511 +/-9 Ma.|||||
39883|Lightning Creek Granite|65396|5|Briefly described|p7, p33, p82, p84, p175, p241, p359,p361|Calymmian|Calymmian|Kalkadoon-Leichhardt Belt: Eastern succession; Williams-Naraku Batholith. Has a prominent magnetic anomaly. p174 implies that most of the ages shown on p175 are U/Pb zircon SHRIMP ages.|1514 +/- 5 Ma, 1511 +/- 9 Ma.|Eureka Supersuite.|||Quartz monzodiorite and monzogranite; also flat-lying quartz-plagioclase aplitic sills associated with magnetite veins.|19-MAR-18
39883|Lightning Creek Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1514 +/- 5 Ma, 1511 +/- 9 Ma|||||
27978|Lightning Creek Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Djungan Volcanic Subgroup of Featherbed Volcanic Group.||||||
27978|Lightning Creek Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Age: 281+/-2 Ma, Rb-Sr. Of Djungan Volcanic Subgroup and Lags Supersuite.||||||
27978|Lightning Creek Rhyolite|23616|5|Briefly described|Table 3 p46|||Of Djungan Volcanic Subgroup/Featherbed Volcanic Group.||||||
27978|Lightning Creek Rhyolite|43087|6|Mentioned|p101|||Of Djungan Volcanic Subgroup.||||||
27978|Lightning Creek Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
27978|Lightning Creek Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Djungan Subgroup.||||||
27978|Lightning Creek Rhyolite|43259|6|Mentioned|Appendix 1,p11.||Early Permian|||||||
27978|Lightning Creek Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
27978|Lightning Creek Rhyolite|43626|2|Defined|p64||Early Permian|Age: 281+/-2 Ma||||||
27978|Lightning Creek Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
27978|Lightning Creek Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Djungan Volcanic Group (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
27978|Lightning Creek Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Djungan Volcanic Subgroup.||Is overlain by Lumma Rhyolite.|Pale to very dark grey, moderately to intensely welded, lithics-poor to very lithics-poor, crystal-rich to extremely crystal-rich, rhyolitic ignimbrite; with clasts of fine-grained, slightly porphyritic rhyolite up to 5 cm.|
27978|Lightning Creek Rhyolite|69593|5|Briefly described|p487 Fig.6.11|||Included in the Lags Supersuite.||Featherbed Volcanic Group.|||Rheomorphic ignimbrite.|
27978|Lightning Creek Rhyolite|71592|5|Briefly described|Appendix A.|||Kennedy igneous Province.|278+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
24358|Lily Creek Sandstone Member|22954|5|Briefly described|p11,19|||||||||
24358|Lily Creek Sandstone Member|40810|5|Briefly described|p14|||[originally entered as NT unit, because mentioned in Amadeus Basin ref. CEB 17FEB95]||||||
24358|Lily Creek Sandstone Member|43807|5|Briefly described|p346|||||||||
24358|Lily Creek Sandstone Member|64068|3|Fully described|p71|Ordovician|Late Cambrian|Contains trilobites and conodonts.  12 m thick.||Top of Chatsworth Limestone.||Is conformably overlain by Ninmaroo Formation.|Massive quartzic limestone; minor calcareous siltstone, bioclastic grainstone.|04-APR-12
24358|Lily Creek Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Late Cambrian|Late Cambrian|Georgina Basin||Cockroach Group|||Calcareous, cross-bedded sandstone, sandy limestone, calcareous siltstone|
27996|Lilyponds Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Matamorphic Group and Rocky King Granite||||||
27996|Lilyponds Granite|43596|4|Described|p31, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Oswald Schist. Pale grey to grey-brown, sparsely porphyritic muscovite-biotite granite.||||||15-JAN-09
27996|Lilyponds Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
36168|Lime Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36168|Lime Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 257. I-Type.||||||
36168|Lime Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36168|Lime Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pink to cream, fine- to medium-grained porphyritic biotite granite. I-type.||||||07-FEB-11
23726|Lindalong Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
23726|Lindalong Granite|22781|4|Described|p34|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
23726|Lindalong Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group||||||
23726|Lindalong Granite|42610|2|Defined|p12|Early Devonian|Early Devonian|Age assumed same as Barwon Granite, about 400Ma.||||||
23726|Lindalong Granite|43738|6|Mentioned|Fig.12,p38|||||||||
23726|Lindalong Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
23727|Lindsay Flat Microgranite|22780|5|Briefly described|map|Late Permian|Early Carboniferous|||||||
23727|Lindsay Flat Microgranite|22781|4|Described|p39|Early Permian|Late Carboniferous|||||||
23727|Lindsay Flat Microgranite|23420|5|Briefly described|p 147 table 4.6|Permian|Late Carboniferous|In the Cape York Penninsula Batholith||||||
23727|Lindsay Flat Microgranite|42610|2|Defined|p30|Permian|Carboniferous|||||||
23727|Lindsay Flat Microgranite|43738|6|Mentioned|Fig.12,p38|||||||||
23727|Lindsay Flat Microgranite|69593|5|Briefly described|p512|||Jardine Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|285 Ma.||||I-type.|
83362|Lineament Prospect dyke|72983|5|Briefly described|p5, p7, p78-79, p81-82|Frasnian|Frasnian|[informal unit name; may be written as Lineament prospect dyke, p78; may be abbreviated as Lineament dyke, p5]. Etheridge Province, Kennedy Igneous Association. Georgetown region. First robust U-Pb isotopic evidence of Late Devonian magmatism within the Etheridge Province.|377.2 +/- 2.0 Ma SHRIMP U-Pb|||Intrudes Forsayth Granite. May be correlated with Mount Darcy microgranodiorite.|Quartz-feldspar porphyry dyke; can host Au mineralisation.|
23729|Linley Rhyolite|9531|5|Briefly described|Map Legend|Permian|Carboniferous|Rhyolitic ignimbrite, tuff.||||||02-JUL-04
23729|Linley Rhyolite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Mount Little Volcanic Group. Age: >/=275Ma. Thickness: 20-50m. Geological Province: Georgetown Region.||||||02-JUL-15
23729|Linley Rhyolite|23430|6|Mentioned|p499|||||||||
23729|Linley Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V1. ?A-Type.||||||
23729|Linley Rhyolite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
23729|Linley Rhyolite|40659|6|Mentioned|p250|||||||||
23729|Linley Rhyolite|40860|4|Described|p110|||||||||
23729|Linley Rhyolite|40954|6|Mentioned|p133|||||||||
23729|Linley Rhyolite|43259|4|Described|Appendix 1,p1.||Permian|||||||
23729|Linley Rhyolite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.|||Pale buff, red-brown or bright green rhyolitic ignimbrite, brecciated in part.|
23729|Linley Rhyolite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.|||Pale buff, red-brown or bright green rhyolitic ignimbrite, brecciated in part.|
23729|Linley Rhyolite|69593|5|Briefly described|p490|Permian|Permian|Kidston Subprovince, Kennedy Igneous Association. Unassigned. Probably A-type.||||||
23730|Lissoy Sandstone|22464|5|Briefly described|p9|Middle Devonian|Middle Devonian|Also p8. Adavale Basin. Overlies Log Creek Formation, overlain by Cooladdi Dolomite||||||
23730|Lissoy Sandstone|22518|6|Mentioned|p 10|||Adavale Basin||||||
23730|Lissoy Sandstone|38226|6|Mentioned|Table 1|||||||||
23730|Lissoy Sandstone|38658|6|Mentioned|p153|||||||||
23730|Lissoy Sandstone|39478|6|Mentioned|Table 1|||||||||
23730|Lissoy Sandstone|39494|6|Mentioned|Fig.3|||||||||
23730|Lissoy Sandstone|40030|6|Mentioned|Fig.3|||||||||
23730|Lissoy Sandstone|40544|6|Mentioned|Fig.4|||||||||
23730|Lissoy Sandstone|41097|6|Mentioned|Table 1|||||||||
23730|Lissoy Sandstone|41167|6|Mentioned|p394|||||||||
23730|Lissoy Sandstone|41198|6|Mentioned|Table 1|||||||||
23730|Lissoy Sandstone|41208|4|Described|p12|||||||||
23730|Lissoy Sandstone|41247|6|Mentioned|Fig.5|||||||||
23730|Lissoy Sandstone|42031|5|Briefly described|Fig.3 P759|||||||||
23730|Lissoy Sandstone|42999|5|Briefly described|Table1,p90|||||||||
23730|Lissoy Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
23730|Lissoy Sandstone|43105|5|Briefly described|p11|||||||||
23730|Lissoy Sandstone|62985|5|Briefly described|p16|Givetian|Givetian|Overlies Log Creek Formation and is laterally equivalent to upper parts of Bury Limestone; unconformably overlain by Etonvale Formation. Feldspathic sandstone and minor siltstones and conglomerates. Geol. prov: Adavale Basin.||||||15-JUL-14
23730|Lissoy Sandstone|64783|3|Fully described|p94-96, 82, 84, 87, 90-93, 98, 100-103|Givetian|Givetian|Of Paten (1977); before then was considered part of the Log Creek Formation. No formal type section exists, although the section in PPC Lissoy-1 (Cores 4 and 5) between 3760m and 3799.6m is promoted informally here as being representative of the unit. Age is early Givetian. Hosts minor hydrocarbons.||||Overlies the Log Creek Formation conformably. Overlies Eastwood beds unconformably or locally conformably. Underlies the Cooladdi Dolomite conformably.|Comprises fine- to coarse-grained feldspathic sandstone and minor siltstone and conglomerate.|15-NOV-17
23730|Lissoy Sandstone|67402|6|Mentioned|p165 tbl LPB1, p166|||Adavale Basin. Proven gas reservoir deposited in a coastal setting. Sediments were deposited in near-shore shallow marine, intertidal or wave zone environments. See also p167 fig ADV/WRR3, p168, p170, fig ADV/WRR7, p172-p175.||||Overlies the Log Creek Formation. Overlain by the Cooladdi Dolomite.|Feldspathic to sub-labile feldspathic sandstones, minor siltstone and conglomerate. Sandstones are fine to coarse grained.|
23730|Lissoy Sandstone|68731|5|Briefly described|p177 Fig 3.91, p180 Tb 3.3|Late Devonian|Middle Devonian|Adavale Basin. Depositional environment discussed. ~ 14.4-166.5 m thick. Contains thin bedding and some laminated beds, soft-sediment deformation, and cross-bedding. Rip-up clasts are also observed. Detailed lithology discussed.||||Merges laterally with the Bury Limestone.|Comprises feldspathic to sub-labile feldspathic sandstone, ranging from grey-green to light red and brown.|
23730|Lissoy Sandstone|72297|5|Briefly described|p746|||Adavale Basin. Hydrocarbon reservoir in the Gilmore gasfield; capped by the Cooladdi Dolomite.||||||
23730|Lissoy Sandstone|73179|6|Mentioned|p1136|||||||||
76895|Lithgow Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite|||Leucogranite, banded pegmatite and aplite|
76895|Lithgow Granite|69591|5|Briefly described|p59|||Sybella Batholith.|1660 +/- 5 Ma (Connors and Page, 1995).||||Leucogranite, banded pegmatite and aplite.|
23731|Little Bird Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered porphyritic biotite granite.||||||02-JUL-04
23731|Little Bird Granite|23291|5|Briefly described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Western Georgetown Region. Age: ca.280Ma. Geological Province: Georgetown Region.||||||02-JUL-15
23731|Little Bird Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 806. S-Type.||||||
23731|Little Bird Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
23731|Little Bird Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23731|Little Bird Granite|40659|6|Mentioned|p250|||||||||
23731|Little Bird Granite|40954|6|Mentioned|p133|||||||||
23731|Little Bird Granite|43259|4|Described|Appendix 1,p52.|Permian|Carboniferous|Middle Proterozoic.||||||03-DEC-13
23731|Little Bird Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||30-JUL-04
23731|Little Bird Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Altered porphyritic biotite granite.|
23731|Little Bird Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Altered porphyritic biotite granite.|
36710|Little Forks Volcanics|23423|4|Described|p308 Table 7.3|Early Permian|Late Carboniferous|Also see p238. Kennedy Igneous Province.||||||
36710|Little Forks Volcanics|50630|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Porphyritic rhyolite and microgranite.||||||
36710|Little Forks Volcanics|60425|5|Briefly described|p50 Tb. 3, p71|Early Permian|Late Carboniferous|Of Donchak et al (1992). Referred to as "Little Forks acid volcanics" by Jones et al(1990).Conflicting interpretations of lithology described (p71). Either unconformable over or intrudes Hodgkinson Fm.||||||07-FEB-11
27645|Little Pocket Dacite|9531|5|Briefly described|Map Legend|Permian|Carboniferous|Porphyritic biotite dacite lava and agglomerate.||||||02-JUL-04
27645|Little Pocket Dacite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Mount Little Volcanic Group. Age: >/=275Ma. Geological Province: Georgetown Region.||||||04-JUN-15
27645|Little Pocket Dacite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanics No. V2. I-Type.||||||
27645|Little Pocket Dacite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
27645|Little Pocket Dacite|40659|6|Mentioned|p250|||||||||
27645|Little Pocket Dacite|40860|4|Described|p110|||||||||
27645|Little Pocket Dacite|40954|6|Mentioned|p133|||||||||
27645|Little Pocket Dacite|43259|4|Described|Appendix 1,p1.||Permian|||||||
27645|Little Pocket Dacite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.||Is overlain conformably by McFarlanes Andesite.|Porphyritic biotite-hornblende dacite lava and agglomerate.|
27645|Little Pocket Dacite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.||Is overlain conformably by McFarlanes Andesite.|Porphyritic biotite-hornblende dacite lava and agglomerate.|
79734|Little Round Back Granite|71792|2|Defined|p26, p28-p29, p42-p43|Devonian|Devonian|Crops out to the west of Portland Roads. Previously mapped as Kintore Granite and partly as Weymouth Granite (Willmott et al, 1973 and Wilmott & Powell, 1977). Hosts auriferous quartz veins in the Scrubby Creek area (part of the Claudie River Gold and Mineral Field). Named after Little Round Back, a prominent hill 283m high in the granite south of Weymouth Bay and directly west of Portland Roads. The type locality occurs at S12.6186', E 143.3862'. This unit has a mottled radiometric response with some areas of high thorium and potassium, this unit is magnetically blind.|409 +/- 6 Ma (Black et al, 1992)|Kintore Supersuite||Intrudes the Sefton Metamorphics. Intruded by the Portland Roads Granite.|S-type granite comprising coarse twinned phenocrysts of microcline in a medium-grained groundmass of quartz, plagioclase and biotite.|
79734|Little Round Back Granite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|||Porphyritic grey biotite granite.|
36523|Little Star Creek complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 176.||||||
41322|Little Toby Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
41322|Little Toby Granite|50536|5|Briefly described|p1.5, 11.2, Table 1.1|||Geological Province: Mount Isa Inlier.  Of the Little Toby Suite.||||||
41322|Little Toby Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot, p6, p30|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. Obsolete name? Not used in GIS. Emplaced in the Ardmore-May Downs Domain, Mount Isa Inlier.|~1810 - 1795 Ma|||Intruded Yaringa Metamorphics.||
41322|Little Toby Granite|69591|5|Briefly described|p30, p32, p60, p105|||Ardmore-May Downs Domain, Mount Isa Province.||Big Toby Suite.||Intrudes Yaringa Metamorphics.|Pink, medium- to coarse-grained biotite granite, locally foliated.|
41322|Little Toby Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
41322|Little Toby Granite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Felsic intrusive.|
30424|Little Watson Granite|23423|6|Mentioned|p305 Table 7.4|||||||||
30424|Little Watson Granite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Ootann Supersuite (Ootann Supersuite).||||||15-JUN-06
30424|Little Watson Granite|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Ootann Supersuite. Geological Province: Kennedy Province. Pale pink to white, fine-grained biotite leucogranite to aplite; commonly altered.||||||
30424|Little Watson Granite|60425|5|Briefly described|p278-9 Appdx|Early Permian|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pale pink to white, medium- to coarse-grained biotite granite.||||||07-FEB-11
30424|Little Watson Granite|62523|5|Briefly described|Map legend at p3-4|Early Permian|Late Carboniferous|Of the Ootann Suite/Ootann Supersuite. Pale pink to white, medium, even-grained, biotite granite to leucogranite.||||||07-FEB-11
38873|Littlemore Granodiorite|23799|5|Briefly described|p117|||Of Littlemore Suite.  Geological Province: Yarrol Province.||||||
38873|Littlemore Granodiorite|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38873|Littlemore Granodiorite|24489|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38873|Littlemore Granodiorite|24615|5|Briefly described|CD|Triassic|Triassic|[Rggi].  Pinkish grey to grey, medium- to coarse-grained biotite-hornblende granodiorite and quartz monzodiorite.||||||
38873|Littlemore Granodiorite|68008|2|Defined|p140, p143, p279, p334, p336, p399|Late Triassic|Late Triassic|See also p401-403, p405, p407, p444, p447, p635, p637. Comprises most of the northern part of Glassford Igneous Complex, along the valley of Ridler Creek. Forms a WSW-trending belt 20 x 6km from Ubobo to Mount Sugarloaf. Named after the Littlemore scheelite mine which occurs within the unit. The type area is along Connell Creek for c.4km upstream from its confluence with Ridler Creek. Variable topography. Geophysics described and modelled: contrasted with Monal Granodiorite. Geochemistry detailed: similar to Lawyer Granite. These K-Ar ages conflict with that of the Robert Granite (230.2 +/- 3.7 Ma) which is believed to intrude the Granodiorite. Hosts the Littlemore scheelite deposit, disseminated copper mineralisation in Mount Roberts area, and copper in skarns with the Rockhampton Group.|221+/-4 Ma; 216+/-4 Ma (Webb and McDougall, 1968)|Glassford Igneous Complex.||Intrudes Rockhampton Group. Is intruded by Ridler Monzonite, Radley Nepheline Syenite, Rule Gabbro and Robert Granite. Is faulted against Calliope beds. Abuts Monal Granodiorite.|Grey, medium- to coarse-grained, equigranular biotite-hornblende granodiorite and quartz monzodiorite. Significant alteration locally.|
38873|Littlemore Granodiorite|68679|5|Briefly described|p427, p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Most extensive unit in the Complex. Geochemistry briefly described.|221 +/- 4 Ma (K-Ar: Webb and McDougall, 1968).|Glassford Igneous Complex.|||Pinkish grey to grey, medium- to coarse-grained biotite-hornblende granodiorite and quartz monzodiorite.|
38873|Littlemore Granodiorite|69594|6|Mentioned|p561|||||||Is intruded by Radley Nepheline Syenite and Ridler Monzonite.||
38873|Littlemore Granodiorite|73450|6|Mentioned|p11, p14, p59, p63|Triassic|Triassic|||||Intruded by Roberts Granite, and Ridler Monzonite and Radley Nepheline Syenite (Glassford Igenous Complex).||
39084|Littlemore Suite|23799|5|Briefly described|p115 Fig. 10, p117|||Of Murray et al (2000, in prep.).  Includes Littlemore Granodiorite, Flaffy Quartz Monzodiorite, Lawyer Granodiorite, Redshirt Granite, Mount Seaviwe Igneous Complex, Craiglands Quartz Monzodiorite and Kabra Quartz Monzodiorite.  Geol.Prov:Yarrol Province||||||
24360|Littleton Dacite Member|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V805. I-Type.||||||
24360|Littleton Dacite Member|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24360|Littleton Dacite Member|40659|2|Defined|p251|Mesoproterozoic|Mesoproterozoic|Of Idalia Rhyolite.||||||21-JUN-04
24360|Littleton Dacite Member|40954|6|Mentioned|p132|||||||||
24360|Littleton Dacite Member|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24360|Littleton Dacite Member|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24360|Littleton Dacite Member|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Very dark grey dacitic ignimbrite, breccia, tuff and lava.|
24360|Littleton Dacite Member|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Idalia Rhyolite.|||Very dark grey dacitic ignimbrite, breccia, tuff and lava.|
30190|Lizard Island Granite|23512|5|Briefly described|Map Legend||Late Permian|of Cooktown Supersuite.||||||
30190|Lizard Island Granite|43111|2|Defined|p46|Late Permian||Of Cooktown Supersuite.||||||
30190|Lizard Island Granite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Cooktown S'suite. S-type.Med-gr.slightly porph.cordierite (altered)-tourmaline-biotite-muscov.granite+leucogranite, with pegmatitic zones+miarolitic cavities; widespread slight to mod. alteration; minor fine-gr., highly porph. garnet-bearing granite.||||||07-FEB-11
30190|Lizard Island Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|||S-type granitoids.|
41783|Lizzie Creek Volcanic Group|60445|6|Mentioned|p5, p37|||Massive conglomerate and andesitic volcanics, sandstone and siltstone in Sandy Creek area. Overlies Connors Volcanic Group. Hosts Mount Britton goldfield.||||||27-NOV-12
41783|Lizzie Creek Volcanic Group|60472|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes the Mount Benmore Volcanics.||||||
41783|Lizzie Creek Volcanic Group|60473|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Carmila beds.||||||17-SEP-04
41783|Lizzie Creek Volcanic Group|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Ametdale Volcanics, Mount Buffalo Rhyolite, Cobweb Mountain Rhyolite, Mount Benmore Volcanics, Carmila beds.||||||
41783|Lizzie Creek Volcanic Group|60479|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Carmila beds.||||||
41783|Lizzie Creek Volcanic Group|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Carmila beds, Mount Benmore Volcanics, Coppermine Andesite, Cobweb Mountain Rhyolite, Mount Buffalo Rhyolite, Tartrus Rhyolite, Ametdale Volcanics.||||||
41783|Lizzie Creek Volcanic Group|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Mount Benmore Volcanics, Mount Buffalo Rhyolite, Langdale Hill Rhyolite, Carmila beds.||||||
41783|Lizzie Creek Volcanic Group|60659|5|Briefly described|p19, p87-88|Early Permian|Early Permian|Of Camboon Volcanic Arc. Comprises andesite, shale, siltstone, rhyolitic volcanics and ignimbrite. Unconformable on Bulgonunna Volcanic Gp; unconformably beneath Mount Wickham Rhyolite. Age: ~284+/-7Ma. Geol Prov: Bowen Basin.||||||07-FEB-11
41783|Lizzie Creek Volcanic Group|61035|4|Described|p3 Fig. 1, p5, p7, p38, p40, p51, p55|Permian|Early Permian|Includes; Carmila beds, Mount Benmore Vol, Cobweb Mountain Rhyolite, Coppermine Andesite, Macksford Andesite, Tartrus Rhyolite, Ametdale Vol, Mount Buffalo Vol, Collaroy Vols + Clements Creek beds. Overlain by Back Creek Group, underlain by Connors Vol.||||||07-FEB-11
41783|Lizzie Creek Volcanic Group|65388|5|Briefly described|p149-150, 85, 86, 90, 32, 53, 83, 106|Early Permian|Early Permian|Connors Arch. Correlated with Camboon Volcanics. Age 285+/- 4 Ma. Includes Cobweb Mountain Rhyolite, Coppermine Andesite, Mount Benmore Volcanics, Ametdale Volcanics, Mount Buffalo Volcanics, Carmila beds, Collaroy Volcanics. Overlain by Tiverton Formation? See also p122, 123, 135, 138, 142, 145, 146, 186, 362, 447.||||||
41783|Lizzie Creek Volcanic Group|65706|4|Described|p11; Tb.1 p15,16,17,18; p51, p54|Early Permian|Early Permian|See also p65, p71, p77-8, p95-6, p123. Parts of this unit probably equivalent to Calen Coal Measures; possibly unconformably overlain by Tiverton Formation and Gebbie Formation (both Back Creek Group). Hosts epithermal Au-Ag-Cu and Au-Cu-Pb-Zn mineralisation; hosts Ag-Pb-Cu mineralisation.|||Includes Carmila beds.|Unconformably overlies Connors Volcanic Group, Bulgonunna Volcanic Group. Intruded by and unconformably underlies Mount Wickham Rhyolite; intruded by Urannah Igneous Complex.|Basaltic to andesitic lavas and volcaniclastic rocks (including breccia, agglomerate and arenite), rhyolitic to dacitic lavas and volcaniclastic rocks (including ignimbrite) and local siltstone, shale and polymictic conglomerate.|
41783|Lizzie Creek Volcanic Group|68359|6|Mentioned|p9|||||||||
41783|Lizzie Creek Volcanic Group|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Connors Subprovince. This unit is mapped with Mount Wickham Rhyolite under the symbol, Pvz.||||||
41783|Lizzie Creek Volcanic Group|68679|4|Described|p312-313, p347, p353, p355, p357-358|Permian|Permian|See also p360-361, p364, p368, p372 Fig.5.64, p375, p379-381, p470. Previously mapped as Lizzie Creek Volcanics (Malone et al. 1964; Dear 1994) and others. Connors Subprovince, northern New England Orogen. Includes all the rocks between the Connors Volcanic Group and the Back Creek Group. Subaerial volcanics; fluvial and lacustrine clastics. Other similar ages given.|283.1+4.5/-2.8 Ma: U-Pb SHRIMP: Cross et al.(2012)||Mount Benmore, Ametdale, Collaroy Volcanics; Carmila {=Goodedulla) beds; Mount Buffalo Rhyolite, Cobweb Mountain Volcanics[=Rhyolite]; Coppermine Andesite.|Is overlain by Collinsville Coal Measures and gradationally by Tiverton Formation.|Basalt, andesite, rhyolite, sandstone and siltstone.|
41783|Lizzie Creek Volcanic Group|68901|4|Described|p2-3, p4, 5, p98-105, p148|Permian|Permian|New England Region. Dates are SHRIMP U-Pb ages and interpreted as the dates of magmatic crystallisation. SHRIMP results and analyses discussed in detail. See also p64, 66, 68, 70,71, p106, 108, 118.|286.9 +/- 2.1 and 283.6 + 4.5/-2.8 Ma|||Interlayered with and intruded by the Mount Wickham Rhyolite.|Dated sample is: Dark grey to dark brown, very fine-grained, moderately porphyritic dacite. Pale-grey, very fine-grained, moderately crystal-rich, lithics poor, dacitic ignimbrite.|15-NOV-18
41783|Lizzie Creek Volcanic Group|69593|5|Briefly described|p497|||Draper and Withnall (1997). Basal unit in northern Bowen Basin; SE of Townsville.||||Equivalent to Julago Volcanics.||
41783|Lizzie Creek Volcanic Group|69952|6|Mentioned|p85|Permian|Permian|||||||
41783|Lizzie Creek Volcanic Group|70673|6|Mentioned|p8-9, p130-131|Permian|Permian|Early Permian.||||Adjacent to Connors Volcanic Group.||
41783|Lizzie Creek Volcanic Group|70740|6|Mentioned|p71, p124|||[Replaces the Lizzie Creek Volcanics?]||||||
41783|Lizzie Creek Volcanic Group|70837|5|Briefly described|p246|Cisuralian|Cisuralian|Of  Bowen Basin. SHRIMP age of 283.1 (Cross etal., 2012). Corresponding to APP3 zone (Cisuralian-Guadalupian).|||Includes Mount Wickham Rhyolite.|||
41783|Lizzie Creek Volcanic Group|71265|5|Briefly described|p589|Kungurian|Kasimovian|Bowen Basin.||||Is overlain by Collinsville Coal Measures.||
41783|Lizzie Creek Volcanic Group|71592|5|Briefly described|Appendix A.|||New England Orogen.|287+/-2.1 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite, ignimbrite.|
41783|Lizzie Creek Volcanic Group|71701|5|Briefly described|p155|Permian|Carboniferous|Northern Area, Bowen Basin.||||Unconformably overlain by the Collinsville Coal Measures.||
41783|Lizzie Creek Volcanic Group|72297|5|Briefly described|p697, p710, p718|Permian|Permian|Hosts the Silver Hill and Mount Carlton high-sulfidation epithermal Au-Ag-Cu prospects in vein systems.||||Is overlain by the Calen Coal Measures.|Includes rhyodacite and volcaniclastics.|
41783|Lizzie Creek Volcanic Group|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||Strathbogie Trachyte, Crush Creek Coal Measures, Mount Toissaint Volcanics and 5 other unnamed sub-units.||Basalt, andesite, interbedded volcaniclastic rocks; generally subordinate dacite, rhyolite, trachyte; conglomerate, labile sandstone, siltstone, calcareous siltstone, shale, carbonaceous shale, locally containing fossil plant fragments; minor coal.|
41783|Lizzie Creek Volcanic Group|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||Includes Mount Benmore Volcanics, Carmila beds.||Includes basalt and andesite, and interbedded volcaniclastic rocks; subordinate dacite, rhyolite, trachyte; conglomerate, labile sandstone, siltstone, calcareous siltstone, shale, locally containing fossil plant fragments; minor coal.|
41783|Lizzie Creek Volcanic Group|73037|5|Briefly described|Map legend|Early Permian|Early Permian||||Includes Mount Benmore Volcanics.||Basalt and andesite, and interbedded volcaniclastic rocks; generally subordinate dacite, rhyolite, trachyte; conglomerate, labile sandstone, siltstone, calcareous siltstone, shale, carbonaceous shale + fossil plant fragments; minor coal + ignimbrite.|
23733|Llandillo Granite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37.||||||
23733|Llandillo Granite|43029|2|Defined|p21||Devonian|see also Fig.2,p16||||||
23733|Llandillo Granite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
23733|Llandillo Granite|43213|3|Fully described|p96-97, p109, p116-121, p175, p178|Devonian|Devonian|See also p208, p219, p233, p241-242. Type locality described. Precise age is unknown; Devonian age is assigned because of similarities with other components of the Retreat Batholith. Peraluminous. Geochemistry, modal and chemical analyses and geophysics detailed.||||Intrudes Annmore Quartz Monzodiorite and Kilmarnock Granodiorite.|Light grey, fine- to medium-grained, equigranular biotite granite, locally with rare hornblende.|
25171|Llewellyn Creek Formation|22460|5|Briefly described|p446, 448|||Also see Fig 1 p446.||||||18-JAN-07
25171|Llewellyn Creek Formation|22467|5|Briefly described|Fig 2 p431.|||Underlain by Fullarton River Group.||||||18-JAN-07
25171|Llewellyn Creek Formation|22513|3|Fully described|P.373-374|||||||||
25171|Llewellyn Creek Formation|22523|5|Briefly described|p365,Fig10p368|||||||||
25171|Llewellyn Creek Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Broken Hill Sundown Group and the Daniel Creek Formation of Georgetown.||||||07-NOV-08
25171|Llewellyn Creek Formation|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1693+/-5Ma.||||||18-JAN-07
25171|Llewellyn Creek Formation|23613|5|Briefly described|p725|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group.||||||07-NOV-08
25171|Llewellyn Creek Formation|23962|5|Briefly described|p1215 Fig. 2|||Geological Province: Mount Isa Inlier.  Of the Soldiers Cap Group.||||||16-DEC-04
25171|Llewellyn Creek Formation|24039|6|Mentioned|p459|||||||||
25171|Llewellyn Creek Formation|24259|6|Mentioned|p115|||Geological Province: Mount Isa Block||||||
25171|Llewellyn Creek Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Soldiers Cap Group. Overlain by Mount Norna Quartzite. Sandstone. Geological Province: Eastern Fold Belt.||||||28-JAN-05
25171|Llewellyn Creek Formation|24462|5|Briefly described|p300|||Of the Soldiers Cap Group.  Geological Province: Mount Isa Block.  Age: 1666 +/- 14 Ma.||||||
25171|Llewellyn Creek Formation|33900|6|Mentioned|p17|||||||||
25171|Llewellyn Creek Formation|35074|6|Mentioned|Fig.2|||||||||
25171|Llewellyn Creek Formation|35295|2|Defined|p601|Carpentarian|Carpentarian|||||||
25171|Llewellyn Creek Formation|37568|5|Briefly described|p81|||||||||
25171|Llewellyn Creek Formation|38276|6|Mentioned|Fig.1|||||||||
25171|Llewellyn Creek Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25171|Llewellyn Creek Formation|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25171|Llewellyn Creek Formation|39445|5|Briefly described|Table 2|||See also p42.||||||18-JAN-07
25171|Llewellyn Creek Formation|39496|5|Briefly described|p7|||||||||
25171|Llewellyn Creek Formation|39622|6|Mentioned|p26|||See also Fig.2||||||
25171|Llewellyn Creek Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25171|Llewellyn Creek Formation|40840|6|Mentioned|Map legend|||||||||
25171|Llewellyn Creek Formation|41464|6|Mentioned|Map legend|Proterozoic||||||||
25171|Llewellyn Creek Formation|41556|6|Mentioned|Map legend|Proterozoic||||||||
25171|Llewellyn Creek Formation|41568|3|Fully described|p6|||||||||
25171|Llewellyn Creek Formation|41791|5|Briefly described|p263|||||||||
25171|Llewellyn Creek Formation|41978|3|Fully described|Table 1 P492|||||||||
25171|Llewellyn Creek Formation|45161|5|Briefly described|Table 12|||||||||
25171|Llewellyn Creek Formation|45166|5|Briefly described|p25|||||||||
25171|Llewellyn Creek Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25171|Llewellyn Creek Formation|50100|5|Briefly described|p11, p13 Fig. 4, p20|Statherian|Statherian|Of the Soldiers Cap Group.  Basal formation in the Cloncurry Subprovince. Overlain by Mount Norna Quartzite. Comprises pelitic schist (with garnet, staurolite and andalusite), phyllite, metagreywacke, quartzite, amphibolite and metabasalt.||||||15-MAR-07
25171|Llewellyn Creek Formation|50125|4|Described|p89|||Of the Soldiers Cap Group. Maximum Thickness: ~2200m. Consists of turbiditic pelite. Conformably overlain by the Mount Norna Quartzite. Geological Province: Mount Isa Inlier||||||18-JAN-07
25171|Llewellyn Creek Formation|50332|4|Described|p16, p21|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group. Age: 1695-1600Ma. Overlain by Mount Norna Quartzite . Basal formation in the Cloncurry Subprovince. Geol Prov: Cloncurry Subprovince. Comprises pelitic schist, phyllite, meatgreywacke, quartzite, amphibolite and metabasalt.||||||07-FEB-11
25171|Llewellyn Creek Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Soldiers Cap Group. Mica schist, phyllite, amphibolite.||||||
25171|Llewellyn Creek Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
25171|Llewellyn Creek Formation|61922|5|Briefly described|p9 Fig. 3, p10, p12 Fig.5, p15-16 Figs.|Paleoproterozoic|Paleoproterozoic|Of Soldiers Cap Group. Quartz-mica psammitic turbidites. Overlies Fullarton River Group; overlain by Mount Norna Quartzite. Age: 1654+/-4Ma. Max. thickness: ~2km. Geol. Prov: Mount Isa Inlier/Eastern Fold Belt.||||||16-APR-12
25171|Llewellyn Creek Formation|61925|5|Briefly described|p56 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||07-NOV-08
25171|Llewellyn Creek Formation|61926|5|Briefly described|p71 Fig. 1, p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
25171|Llewellyn Creek Formation|61927|5|Briefly described|p93, p95|||Metasedimentary unit.||||||
25171|Llewellyn Creek Formation|61929|5|Briefly described|p127, p129 Fig. 3|||Of the Soldiers Cap Group. Bedded quartz-mica psammite and pelite with graded turbidic cycles. Geological Province: Calvert Superbasin.||||||
25171|Llewellyn Creek Formation|61936|5|Briefly described|p195 Fig. 6|||Include turbidites. Age: <1712Ma. Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
25171|Llewellyn Creek Formation|62047|6|Mentioned|p91 Fig.2 |||||||||
25171|Llewellyn Creek Formation|63866|5|Briefly described|p63|Statherian|Statherian|Records a range in metamorphic grade from amphibolite facies to granulite facies.|c. 1685 Ma|Soldiers Cap Group||||
25171|Llewellyn Creek Formation|64248|6|Mentioned|p36, p38 Fig.5, p43|Statherian|Statherian|Appears as Lewellyn on p36 and p43. Foster and Austin (2008) proposed moving this unit out of and below Soldiers Cap Group. Ages are for Snake Creek and Middle Creek respectively.|>1686 +/- 8 Ma and 1666 +/- 14 Ma.|||Overlain by Soldiers Cap Group.||11-DEC-17
25171|Llewellyn Creek Formation|64249|6|Mentioned|p84 Fig. 2, p101, p103|||Geological Province: Mount Isa Inlier.||||||22-APR-09
25171|Llewellyn Creek Formation|64250|5|Briefly described|p7, p11-13 figs 3-5, p19, p27|||The problem of the age of this unit is discussed in detail, as it is intruded by a 1686 +/- 8 Ma tonalite yet includes  a <1666 +/- 14 Ma detrital zircon.||Oldest part of Soldiers Cap Group.||||
25171|Llewellyn Creek Formation|64252|5|Briefly described|p70 Fig. 1, p71, p77|||Of Soldiers Cap Group. Geological Province: Mount Isa Inlier. Metaturbidites.||||||
25171|Llewellyn Creek Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
25171|Llewellyn Creek Formation|65396|4|Described|p7, p12, p15-17, p79, p82, p84, p101-102|Statherian|Statherian|See also p105, p107, p118, p161, p169, p175-178, p183, p187, p190, p195-198, p202, p217, p222, p241, p356, p439-440. Snake Creek Anticline, Calvert Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. The authors propose moving this unit out of and below the Soldiers Cap Group. Detrital zircon sources listed. Age problems discussed, with a tonalite intrusion dated at 1686 +/- 8 Ma (SHRIMP U-Pb: Fanning). Is correlated with Kuridala Formation(?)|<1666 +/- 14 Ma [??]|Basal Soldiers Cap Group.||Overlies Gandry Dam Gneiss, conformably overlies Fullarton River Group. Is conformably/unconformably overlain by Mount Norna Quartzite; overlain by Toole Creek Volcanics.|Thick bedded turbidites: interlayered metapsammites and andalusite schists; layered gabbro and intrusive igneous rocks.|04-APR-17
25171|Llewellyn Creek Formation|65755|6|Mentioned|p2|||Part of Soldiers Cap Group in the north, Cloncurry Fault Zone.||||||
25171|Llewellyn Creek Formation|65887|5|Briefly described|p51|||Basal unit of Soldiers Cap Group. Conformably overlain by Mount Norna Quartzite. Turbiditic pelite and lesser metadolerite.||||||
25171|Llewellyn Creek Formation|66913|5|Briefly described|p170 fig 1, p172|||Mineralisation? 1690-1650 Ma|Deposition 1710-1670 Ma. |Of Soldiers Cap Group.|||Includes turbidites, quartzite, basalt, and dolerite.|
25171|Llewellyn Creek Formation|67323|4|Described|Solid Geology Map, p19, p21|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin. Appears as Llewellyn Formation on p19 and p21. A mafic sill was dated at 1678 +/- 5 Ma (Rubenach et al., 2008).|~1685 Ma (MDA: Neumann et al., 2009).|Soldiers Cap Group.||Correlated with Starcross Formation.|Pelitic schist containing garnet, staurolite and andalusite; phyllite, metagreywacke, quartzite, amphibolite|
25171|Llewellyn Creek Formation|67498|5|Briefly described|p919, 920, p925 Fig.4, p924, 929, 932|||||Of the Soldiers Cap Group.|||Pelitic schist with garnet, staurolite and andalusite; phyllite, metagreywacke, quartzite and amphibolite.|
25171|Llewellyn Creek Formation|67539|4|Described|p13|Statherian|Statherian|Basal unit. Detrital zircon age.|c. 1670 - 1650 Ma|Of the Soldiers Cap Group.||Equivalent of the Answer Slate. Overlain by the Mount Norna Quartzite?||
25171|Llewellyn Creek Formation|68146|5|Briefly described|p4, p113-114, p201|||Has many similarities to, and is tentatively correlated with, Starcross Formation. MDA by Neumann et al. (2009). Minimum age constrained by a tonalite intrusion dated at 1678 +/- 5 Ma (Rubenach et al., 2008; Neumann et al., 2009).|1692 +/- 8 Ma maximum depositional age.|Basal Soldiers Cap Group.||Is overlain by Mount Norna Quartzite.||
25171|Llewellyn Creek Formation|68542|6|Mentioned|p16 fig 4|||||||||
25171|Llewellyn Creek Formation|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 3 (1690-1650 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
25171|Llewellyn Creek Formation|68732|5|Briefly described|p163, p164, p165 Fig.5, p167|Statherian|Statherian|Detrital zircon maximum sedimentary depositional age. A tonalite body in this Formation was dated at 1686 +/- 8 Ma (Rubenach et al., 2008).|1681 +/- 10 Ma|Of the Soldiers Gap Group.|||Sandstones grading up into laminated siltstones and shales; packages several kilometres thick.|30-NOV-17
25171|Llewellyn Creek Formation|69056|5|Briefly described|p4, p13, p55, Time-Space plot sheet|Statherian|Statherian|Soldiers Cap Domain. Detrital zircon maximum depositional age.|~1685 Ma (Neumann et al., 2009).|Soldiers Cap Group.|||Meta-turbidites. Metamorphic grade increases from greenschist to gneiss and migmatites S of Snake Creek area.|
25171|Llewellyn Creek Formation|69370|5|Briefly described|p307, p309-312, p314-315|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block. Appears in Fig.2 as Lewellyn Creek Formation. Intruded by a thick gabbroic to tonalitic sill dated 1686 +/- 8 Ma. Deformation described in detail.||Unit in Soldiers Cap Group.||Is overlain by Mount Norna Quartzite.|Pelitic to psammo-pelitic metaturbiditic unit hosting multiple porphyroblastic mineral phases.|25-JAN-19
25171|Llewellyn Creek Formation|69591|4|Described|p38 Fig.2.22, p41, p43, p55|||Soldiers Cap Domain, Calvert Superbasin. Part of Prize and Gun Supersequences. Submarine fan deposits. Metamorphic grade increasing southwards into gneiss and migmatite. Lacks the bluish quartzite that distinguishes Mount Norna Quartzite high-grade rocks. SHRIMP detrital zircon age. Trondhjemite in a mafic sill was dated at 1678 +/- 5 Ma (Rubenach et al., 2005).|1681 +/- 10 Ma (MDA: Neumann et al., 2009).|Soldiers Cap Group.||Is overlain by Mount Norna Quartzite. Is intruded by Toole Creek Volcanics sills.|Pelitic schist containing garnet, staurolite and andalusite; phyllite, metagreywacke, quartzite, amphibolite.|
25171|Llewellyn Creek Formation|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Is overlain by Mount Norna Quartzite.|Pelitic schist containing garnet, staurolite and andalusite interbedded with metapsammite and quartzite.|
25171|Llewellyn Creek Formation|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Is overlain by Mount Norna Quartzite.|Pelitic schist containing garnet, staurolite and andalusite interbedded with metapsammite and quartzite.|
25171|Llewellyn Creek Formation|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Basal Soldiers Cap Group.||Is overlain by Mount Norna Quartzite.|Pelitic schist containing garnet, staurolite and andalusite interbedded with metapsammite and quartzite.|05-MAY-16
25171|Llewellyn Creek Formation|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group.|||Pelitic schist containing garnet, staurolite and andalusite interbedded with metapsammite and quartzite.|
25171|Llewellyn Creek Formation|71592|5|Briefly described|Appendix A.|||Soldiers Cap Domain, Mount Isa Orogen. Metamorphosed at 1599 +/- 10 Ma (U-Pb monazite SHRIMP).|1681+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite, sandstone.|
25171|Llewellyn Creek Formation|72889|5|Briefly described|p33, p35-p36.|||||Soldiers Cap Group||Along with Mount Norna Quartzite,  correlated with of Starcross Formation.||25-NOV-20
25171|Llewellyn Creek Formation|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
25171|Llewellyn Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Snake Creek-Soldiers Cap Domain.|1693+/-5 Ma, 1681+/-10 Ma max. depositional ages||||Siliciclastics, includes mafic extrusives and carbonaceous siliciclastics.|
24361|Loafers Granodiorite|23220|5|Briefly described|Fig.2, p13|Early Devonian|Late Silurian|||||||
24361|Loafers Granodiorite|23291|5|Briefly described|p35|Devonian|Silurian|Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||18-JUN-15
24361|Loafers Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 45. I-Type.||||||
24361|Loafers Granodiorite|35920|2|Defined|p24|Carboniferous|Silurian|Late Proterozoic or Silurian-Devonian or Carboniferous||||||
24361|Loafers Granodiorite|36937|6|Mentioned|p229|||||||||
24361|Loafers Granodiorite|37570|4|Described|p121|||||||||
24361|Loafers Granodiorite|37576|5|Briefly described|p8|||||||||
24361|Loafers Granodiorite|39445|6|Mentioned|p72|||See also P148||||||
24361|Loafers Granodiorite|39917|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
24361|Loafers Granodiorite|43259|4|Described|Appendix 1,p18.|Early Devonian|Late Silurian|||||||
24361|Loafers Granodiorite|50211|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pinkish-grey, locally weakly foliated, medium-grained biotite-hornblende granodiorite. Of the Glenmore Batholith.||||||18-JUN-15
24361|Loafers Granodiorite|68357|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Glenmore Batholith, Pama Province.|||||Pinkish-grey, locally weakly foliated, medium-grained biotite-hornblende granodiorite.|
24361|Loafers Granodiorite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
27467|Lochaber Granite|23032|4|Described|p45||Early Carboniferous|||||||
27467|Lochaber Granite|23291|4|Described|p46, p97 Tb. 3.11|Carboniferous|Carboniferous|Age: 340+/-3Ma (SHRIMP). Intrudes the Eastdale Granite and is intruded by Sues Creek Microgranite. Parent: Glenmore Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27467|Lochaber Granite|23430|5|Briefly described|p489|||SHRIMP zircon 340.3 +/- 3.8 Ma. Kennedy Province.||||||
27467|Lochaber Granite|23453|5|Briefly described|p12 Tab.1|Dinantian|Dinantian|340+/-3Ma||||||
27467|Lochaber Granite|23494|5|Briefly described|p19 Tb. 1|Triassic|Permian|Intrudes Forsayth and Dumbano Granites.||||||
27467|Lochaber Granite|23498|5|Briefly described|p20 table 1||Permian|||||||
27467|Lochaber Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No.35. I-Type.||||||
27467|Lochaber Granite|23619|4|Described|p40 Table 2||Carboniferous|Of Lochaber Ring Complex.||||||
27467|Lochaber Granite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
27467|Lochaber Granite|31832|6|Mentioned|Table 6|||||||||
27467|Lochaber Granite|32553|4|Described|p58|||||||||
27467|Lochaber Granite|33669|6|Mentioned|p518|||||||||
27467|Lochaber Granite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
27467|Lochaber Granite|39445|5|Briefly described|Table 12|||||||||
27467|Lochaber Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27467|Lochaber Granite|41272|5|Briefly described|p27|||See also M1of 1 H05||||||21-MAY-15
27467|Lochaber Granite|43113|4|Described|Table 2 p25||Carboniferous|of Lochaber Ring Complex||||||
27467|Lochaber Granite|43253|5|Briefly described|map legend||Carboniferous|||||||
27467|Lochaber Granite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
27467|Lochaber Granite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
27467|Lochaber Granite|43664|6|Mentioned|p83||Carboniferous|||||||
27467|Lochaber Granite|43716|6|Mentioned|p105|||||||||
27467|Lochaber Granite|43740|4|Described|p27||Carboniferous|||||||
27467|Lochaber Granite|44048|14|Not recorded|Map Legend||Permian|(Triassic?)||||||
27467|Lochaber Granite|44049|14|Not recorded|Map Legend||Permian|(Triassic?)||||||
27467|Lochaber Granite|44053|2|Defined|p241-243,Fig.33|||||||||
27467|Lochaber Granite|44059|14|Not recorded|p442(Tb)|Permian|Carboniferous|||||||
27467|Lochaber Granite|44542|2|Defined|p27,28|Late Paleozoic|Early Paleozoic|Genetically related to Butlers Igneous Complex and Glenmore Ring Dyke Complex. (Middle Palaeozoic-Late Palaeozoic)||||||17-JUN-13
27467|Lochaber Granite|45003|14|Not recorded|p15|||||||||
27467|Lochaber Granite|45009|14|Not recorded|p24,75,105-6,132,||Permian|Pl.13,Tb.13. Forms core of Bagstowe Ring Dyke Complex.||||||
27467|Lochaber Granite|45014|2|Defined|p79-81,93,97-8,121-2|Permian|Carboniferous|Pl.20,21,38,42,Tb.1. Probably Carboniferous-Permian.||||||
27467|Lochaber Granite|45087|6|Mentioned|p18|||Chemical analyses||||||
27467|Lochaber Granite|45113|6|Mentioned|p11|||||||||
27467|Lochaber Granite|46845|6|Mentioned|Table 1|||||||||
27467|Lochaber Granite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27467|Lochaber Granite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27467|Lochaber Granite|67113|6|Mentioned|p408 Fig.2|||Georgetown Inlier, Australian Craton.|337.9 Ma.|||||
27467|Lochaber Granite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Unit in Lochaber Ring Structure.|||||Pink, fine- to medium-grained biotite granite.|
27467|Lochaber Granite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure. Contains 3 unnamed subunits.|||||Pink, fine to medium-grained biotite granite; complex of rhyolite cone sheets intruding microgranite.|
27467|Lochaber Granite|69593|5|Briefly described|p490|||Kidston Subprovince, Kennedy Igneous Association.|~345-335 Ma (SHRIMP U-Pb zircon ages).|Glenmore Supersuite.|||(Hornblende-)biotite and biotite granite; locally strongly miarolitic; some accessory topaz and fluorite. I-type.|
23734|Locharwood Rhyolite|22675|4|Described|p56|Late Carboniferous|Carboniferous|Bulgonunna Volcanic Group||||||
23734|Locharwood Rhyolite|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23734|Locharwood Rhyolite|23161|4|Described|p19,20 table3||Late Carboniferous|||||||
23734|Locharwood Rhyolite|23504|5|Briefly described|Map Legend||Carboniferous|Of Bulgonunna Volcanic Group.||||||15-MAR-13
23734|Locharwood Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V73. I-Type.||||||
23734|Locharwood Rhyolite|42701|3|Fully described|p36|||||||||
23734|Locharwood Rhyolite|43259|4|Described|Appendix 1,p7.||Late Carboniferous|of Bulgonunna Volcanic Group. U-Pb zircon age of 308+/-2 Ma.||||||
23734|Locharwood Rhyolite|43391|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Bulgonuna Volcanic Group. Geological Province: Coastal Ranges Igneous Province.  Rhyolitic ignimbrite with red fiamme.||||||23-JUN-04
23734|Locharwood Rhyolite|43706|5|Briefly described|p6||Late Carboniferous|||||||
23734|Locharwood Rhyolite|43727|5|Briefly described|Table 14,p50|||||||||
23734|Locharwood Rhyolite|43734|5|Briefly described|Fig.2,p2|||U-Pb age: 304.7+/-6.2 Ma||||||
23734|Locharwood Rhyolite|43936|5|Briefly described|Map Legend||Carboniferous|Of Bulgonunna Volcanic Group||||||
23734|Locharwood Rhyolite|44245|5|Briefly described|Map Legend||Carboniferous|||||||
23734|Locharwood Rhyolite|60659|5|Briefly described|p16, p79|Late carboniferous|Late Carboniferous|Of Bulgonunna Volcanic Gp. Mainly densely welded, moderately crystal-rich rhyolitic ingminbrite. Overlies Mount Coolon Andesite; underlies Pinang Rhyolite. Age: 304.7+/-6.2Ma. Part of the Locharwood association; of the Bulgonunna Province.||||||07-FEB-11
23734|Locharwood Rhyolite|66086|5|Briefly described|Map legend|Carboniferous|Carboniferous|Moderately crystal-rich to crystal-rich rhyolitic ignimbrite, well-developed eutaxitic texture.||||||
23734|Locharwood Rhyolite|68404|5|Briefly described|Map legend|Carboniferous|Carboniferous|Drummond Basin|||||Moderately crystal-rich to rhyolitic ignimbrite, well developed eutaxitic texture.|
23734|Locharwood Rhyolite|68901|5|Briefly described|p114|||SHRIMP age are derived from Black, 1994.|304.7 +/- 6.2 Ma  (SHRIMP U-Pb)|||Equivalent to the Pyramid Rhyolite.|Rhyolitic ignimbrite.|27-SEP-18
23734|Locharwood Rhyolite|69593|5|Briefly described|p495, p513|Permian|Late Carboniferous|Burdekin Falls Subprovince, Kennedy Igneous Association. The LITHOLOGY description is for the whole Group. Sm-Nd isotope data tabulated.|305 +/- 6 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments. I-type.|
23734|Locharwood Rhyolite|70740|3|Fully described|iv, p8, p82 fig 50, p83, p84|Carboniferous|Carboniferous|Drummond Basin. Replaced in part by the Hidden Valley Rhyolite. SHRIMP age derived from Black (1994) although it is unclear whether this age is from the main mapped body or not. Probably intruded by the Bluegrass Creek Granite. Mistakenly referred to as the Locharwood rhyolite on p87. Previously incorporated rocks which have now been named the Hidden Valley Rhyolite (based on geochemical differences between the two units). Divided into a number of informal sub-units. A type locality is nominated and only very briefly described. Distribution and petrography are discussed. See also p87, p88, p99-p102, p104 fig 60, p106, p129.|304.7 +/- 6.2 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Overlies the Bimurra Volcanics. Overlain by the Pinang Rhyolite and the Suttor Formation.|Monotonous, moderately crystal-rich, strongly welded rhyolitic ignimbrite with sparse felsic volcanic lithic fragments.|
23734|Locharwood Rhyolite|71592|5|Briefly described|Appendix A.|||Drummond Basin.|305+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite, welded ignimbrite.|
23734|Locharwood Rhyolite|73035|5|Briefly described|Map legend|Carboniferous|Carboniferous|Some polygons of this unit are uncertainly identifed.|||||Moderately crystal rich to crystal rich rhyolitic ignimbrite, well developed eutaxitic texture.|
39682|Lochenbar Formation|24399|5|Briefly described|p275, p272 Fig. 1|Late Devonian|Late Devonian|Volcaniclastic sediments, minor limestone and varying proportions of primary volvanic rocks.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt.||||||
39682|Lochenbar Formation|24615|5|Briefly described|CD|Late Devonian|Late Devonian|[Dl].  Green-grey to purple granule to cobble andesitic breccia and lesser conglomerate, fine- to medium-grained feldspathic sandstone, fine to medium locally amygdaloidal locally porphyritic andesite, siltstone.||||||
39682|Lochenbar Formation|50197|5|Briefly described|Map Legend|Devonian|Devonian|||||||
39682|Lochenbar Formation|50214|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Overlies the Marble Waterhole beds; underlies Three Moon Conglomerate.||||||17-MAY-04
39682|Lochenbar Formation|61147|6|Mentioned|p383. |Frasnian|Frasnian|Limestones span four conodont zones, equating with the last half of the Frasnian.||||||
39682|Lochenbar Formation|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Late Devonian|Dominant rock type is volcanic conglomerate with clasts of basaltic to andesitic composition; with coral and conodont faunas in limestone lenses, brachiopods in clastic rocks indicating a marine environment. Geol Prov: Yarrol Province.||||||
39682|Lochenbar Formation|63600|5|Briefly described|p900 Fig. 1, p915|Early Carboniferous|Late Devonian|Part of the volcanic/sedimentary sequences unconformably overlying Capella Creek Group.||||||07-FEB-11
39682|Lochenbar Formation|65388|5|Briefly described|p39, 38, 42, 68, 72, 158, 323|Late Devonian|Late Devonian|Metamorphosed by Kariboe Layered Gabbro. Geochemical evidence suggests may be equivalent to all or part of Yaparaba Volcanics. Structurally interleaved with Late Devonian Three Moon Conglomerate. See also Lochenbar Suite p67, 72.||||||
39682|Lochenbar Formation|68008|2|Defined|p1, p43-44, p48, p50, p52, p61, p63-67|Famennian|Frasnian|See also p69, p71, p77, p79-80, p90, p109, p131, p209, p294, p433, p435, p477, p479, p488, p573, p580-581, p588, p602-603. Includes all of the former Dawes Range Formation and most of the Kroombit beds (Dear, 1968; Dear et al., 1971). Forms a SE-trending belt 50km long and up to 15km wide. Named after Lochenbar homestead. The type section is a 610m conformable sequence S of the homestead, from GR276768 7293247 to GR276585 7292248. Forms flat to moderately hilly country. Geophysical responses described; compared with Kariboe Gabbro. Geochemistry described and discussed. Mature island-arc deposits. Coral species listed. Correlated with Channer Creek beds. At least partly equivalent to Mount Hoopbound, Balaclava, Mount Alma Formations and Three Moon Conglomerate. Hosts the Old Kroombit mine. Micropaleontology table. Shelly fossils listed.||||Is overlain unconformably by Youlambie Conglomerate and Winterbourne Volcanics. Is faulted against Marble Waterhole beds. Is intruded by Wingfield Granite and Kariboe Layered Gabbro (=Kariboe Gabbro).|Generally purple- to grey-coloured rocks. Dominated by granule to cobble epiclastic (volcaniclastic) rocks of basaltic to andesitic, lesser dacitic, composition; basaltic andesites and basalts; two large bodies of fossiliferous limestone.|
39682|Lochenbar Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Balaclava and Mount Hoopbound Formations, the Tanderra Volcanics,  the Channer Creek beds and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
39682|Lochenbar Formation|68679|5|Briefly described|p310, p312-313, p316, p337-338, p344|Famennian|Frasnian|See also p348-349, p416, p419, p468. Murray et al. (2012). Originally the upper part of the Kroombit beds of Dear (1968), later expanded by Dear, McKellar and Tucker (1971). Yarrol Province. Part of the Rawbelle Batholith. Basalts are typical of mature island arcs. Chemically similar to Tanderra Volcanics. Shallow-marine to subaerial deposits.||||Is intruded by Kariboe Layered Gabbro. Is faulted against Marble Waterhole beds. May be equivalent to the Yaparaba Volcanics.|Mainly granule to cobble conglomerate with clasts of epiclastic (volcaniclastic), basaltic to andesitic and lesser dacitic rocks with some polymict examples; minor limestones form large, richly fossiliferous outcrops.|
40860|Lochlea Metarhyolite|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Of the Balcooma Metavolcanic Group.  Dark grey, strongly foliated metarhyolite (possibly ignimbrite) containing sparse plagioclase phenocrysts.||||||
40860|Lochlea Metarhyolite|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.||Unit in Balcooma Metavolcanic Group.|||Dark grey, strongly foliated metarhyolite (possibly ignimbrite) containing sparse plagioclase phenocrysts.|
40860|Lochlea Metarhyolite|68731|5|Briefly described|p152, p154|Early Ordovician|Early Ordovician|Includes preserved ghost shards, lithic clasts, and widespread lenticular fabric (uncertain origin). Sedimentary rocks are rare but include lithic metasandstone and siltstone. Age constrained by the parent Balcooma Metavolcanic Group.||Of the Balcooma Metavolcanic Group.|||Comprises crystal-poor metarhyolite with sparse plagioclase phenocrysts in a recrystallised fine-grained groundmass.|
22209|Lochs Gneiss|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Coen Metamorphic Group||||||12-JAN-05
22209|Lochs Gneiss|22781|4|Described|p25,13|Mesoproterozoic|Mesoproterozoic|Coen Metamorphic Group||||||12-JAN-05
22209|Lochs Gneiss|23420|5|Briefly described|p 142 table 4.4||Mesoproterozoic|Age: 1544+/-Ma. In the Coen Metamorphic Group||||||
22209|Lochs Gneiss|43738|6|Mentioned|p37|||||||||
22209|Lochs Gneiss|69591|4|Described|p77 Fig.2.76, p78 Tb.2.6|||Savannah Province, Coen Inlier.|1554 +/- 4 Ma in situ partial melting.|Coen Metamorphic Group.||Grades into Goolha-Goolha and Yarraden Schists.|Sillimanite-mica-feldspar gneiss, grades into schist. May include orthogneiss(?).|
22209|Lochs Gneiss|71792|3|Fully described|p3, p5-p6, p10, p31|Mesoproterozoic|Mesoproterozoic|Coen Inlier, Savannah Province. Named for the Lochs Creek on the Ebagoola 1:100k sheet. Forms a largely concealed belt 140km long through the central Coen Inlier. A metamorphic crystallisation age of 425 +/- 9 Ma (Cross et al, in prep). Extended to include outcrops on the southern side of the Archer River Shear Zone, these rocks were previously mapped as Holroyd Metamorphics of Willmot et al (1973). Structure and petrology is discussed. Characterised my moderate magnetic response and in radiometrics pale green to aqua tones. Also referred to as the Loch Gneiss on p31.|1591 Ma +/- 8 Ma (Max. deposition age)|Coen Metamorphic Group||Conformably (gradationally) overlies the Yarraden Schist.|Grey, medium- coarse-grained, equigranular biotite-muscovite-feldspar gneiss grading into schist and occasional amphibolite.|
22209|Lochs Gneiss|71849|6|Mentioned|p8,p15,p19,p84,p86,p108,p124-125,p195|Mesoproterozoic|Paleoproterozoic|Previously (part of) Coen Metamorphics.||Coen Metamorphic Group.||||
22209|Lochs Gneiss|71853|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.||In places gradational into Yarraden Schist and Goolha-Goolha Schist.|Biotite-muscovite-feldspar gneiss; with sillimanite, garnet, chlorite, epidote and rare chiastolite, kyanite.|
22209|Lochs Gneiss|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.|||Biotite-muscovite-feldspar gneiss; with sillimanite, garnet, chlorite, epidote and rare chiastolite, kyanite; in places gradational into Yarraden Schist and Goolha-Goolha Schist.|
22209|Lochs Gneiss|72983|4|Described|p6-7, p52, p83, p86-89|Calymmian|Calymmian|Iron Range Province. Eastern Cape York region. New work led to a sampled outcrop mapped as Holroyd Group being reassigned to this unit. Listed date is a maximum depositional age. Metamorphic age of 425 +/- 9 Ma. Ages also indicate an early Mesoproterozoic thermal event with an interpreted minimum age of 1500 Ma, as well as a younger Paleozoic thermal event at ~425 Ma. Hosts Au quartz vein mineralisation [near contact with Queenslander Reef dyke?].|1591 +/- 8 Ma SHRIMP U-Pb|Coen Metamorphic Group||Intruded by Queenslander Reef dyke.|Psammitic to pelitic biotite gneiss and minor amphibolite, rare sillimanite and pods of quartz muscovite pegmatite.|
22209|Lochs Gneiss|73387|6|Mentioned|p1|Calymmian|Calymmian|Maximum depositional age of 1591 +/- 8 Ma from Cross et al. (2019).|1591 +/- 8 Ma|Coen Metamorphic Group||||
79733|Lockhart River Granite|71792|2|Defined|p33, p48-p49|Early Permian|Early Permian|Northern Coen Inlier. This unit was previously included as part of the Weymouth Granite. Forms prominent bouldery outcrops in the area around the foreshore of Lloyd Bay, east of Lockhart River Township for which it is named. The type locality is proposed at field point QFG8052 (S 12.7951', E 143.3596'). Distribution and geophysical characteristics are discussed. Considered to be an I-type granite. Interpreted to be overlain by Quaternary coastal sediments.||Weymouth Supersuite||Intrudes the Sefton Metamorphics.|Pink coarse-grained porphyritic hornblende-biotite syenogranite.|
79733|Lockhart River Granite|71853|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||Pink, coarse-grained porphyritic hornblende-biotite granite.|
23736|Lomandra Limestone|23032|5|Briefly described|p27 fig6|Devonian|Devonian|||||||
23736|Lomandra Limestone|23423|5|Briefly described|Plate 8.4a|||Wando Vale Subgroup||||||
23736|Lomandra Limestone|23424|5|Briefly described|Table 8.1|Givetian|Emsian|Of Wando Vale Subgroup/Broken River Group, Graveyard Creek Subprovince.||||||
23736|Lomandra Limestone|23522|5|Briefly described|p250 Fig 6|Eifelian|Emsian|||||||
23736|Lomandra Limestone|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Givetian|Eifelian|Of the Broken River Group. Overlain by the Storm Hill Sandstone. Overlies the Bracteata Formation. Limestone is Ls in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
23736|Lomandra Limestone|24611|6|Mentioned|p194|Emsian|Emsian|Of the Broken River Group.||||||
23736|Lomandra Limestone|41260|3|Fully described|Table 1|||Described P119 and Table 1||||||
23736|Lomandra Limestone|41679|2|Defined|p258|Eifelian|Emsian|Age: late Emsian to early Eifelian.||||||
23736|Lomandra Limestone|41719|6|Mentioned|Fig.2|||||||||
23736|Lomandra Limestone|41739|6|Mentioned|Fig.2|||||||||
23736|Lomandra Limestone|41740|6|Mentioned|p222|||||||||
23736|Lomandra Limestone|42015|6|Mentioned|p318|||||||||
23736|Lomandra Limestone|42032|6|Mentioned|p505|||||||||
23736|Lomandra Limestone|42054|6|Mentioned|p273|||||||||
23736|Lomandra Limestone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
23736|Lomandra Limestone|42933|3|Fully described|Table 2|||See also p102.||||||19-MAR-08
23736|Lomandra Limestone|50093|4|Described|p237, p329 Fig.2, p330 Fig.3|Eifelian|Emsian; Serolinus zone (conodont)|Overlies Bracteata Formation, overlain by Storm Hill Sandstone. Of Broken River Group.||||||07-FEB-11
23736|Lomandra Limestone|63152|5|Briefly described|p120 Fig. 3|Eifelian|Emsian|Of the Broken River Group. Age is late Emsian to early Eifelian. Highly fossiliferous, lithologically diverse carbonate complex.||||||10-APR-07
23736|Lomandra Limestone|65214|6|Mentioned|p272, p277|Devonian|Devonian|QLD NORTH and Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
23736|Lomandra Limestone|68336|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; minor calcareous siltstone, mudstone and sandstone and polymictic conglomerate.|
23736|Lomandra Limestone|68341|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; minor calcareous siltstone, mudstone and sandstone and polymictic conglomerate.|
23736|Lomandra Limestone|68478|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; minor calcareous siltstone, mudstone and sandstone and polymictic conglomerate.|
23736|Lomandra Limestone|68479|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Bioclastic calcarenite, calcirudite and calcilutite; minor calcareous siltstone, mudstone and sandstone and polymictic conglomerate.|
23736|Lomandra Limestone|69592|5|Briefly described|p264, p266|Eifelian|Emsian|Southern Graveyard Creek Subprovince, Broken River Province. Up to 430m thick. Open marine shelf deposits, with a gradient to the NE. Age range from macrofauna and conodonts. See also reference to Lomandra Formation (p259).||Wandovale Subgroup.||Overlies Bracteata Mudstone. Is overlain conformably by Storm Hill Sandstone or, where absent, Dosey Limestone. Interfingers with Burges Formation.|Thin- to medium-bedded bioclastic limestone (from lime mudstone, commonly bioturbated, to calcirudite); minor terrigenous calcareous mudstone and sandstone, and rare quartz sandstone and pebble conglomerate lenses.|
78935|Lonesome Creek Quartz Monzodiorite|65388|3|Fully described|p264, p236 Fig. 81, p254|Early Permian|Late Carboniferous|Replaces Lonesome Creek Monzonite. Shape of the mapped contact suggests is intruded by the Parraweena Gabbro. Relationship with Glenhalvern Granite [and the Shawlands Granite Complex] is unclear. Age likely to be Late Carboniferous, based on similarity to Glandore Granodiorite. Pale pink, green and grey, medium-grained, hornblende-biotite quartz monzodiorite or quartz monzonite.||||||
78935|Lonesome Creek Quartz Monzodiorite|68679|5|Briefly described|p407-408|Late Carboniferous|Late Carboniferous|Auburn Subprovince, New England Orogen. Probable intrusive relationship is based on the shape of the mapped contact. Age is based on similarity to Glandore Granodiorite.||||Probably intruded by Parraweena Gabbro.|Pink and green hornblende-biotite monzodiorite; greyish-white and green, medium-grained granodiorite; orange-pink and green, medium-grained hornblende-biotite monzonite to syenite.|
22213|Long Gully Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
22213|Long Gully Granite|23616|6|Mentioned|p71 Fig 13|||Of Almaden Supersuite.||||||
22213|Long Gully Granite|23713|5|Briefly described|p74 Appendix 2|||||||||
22213|Long Gully Granite|24485|5|Briefly described|p52 Tb.8|Late Carboniferous|Late Carboniferous|Intrudes the Ruddygore Granodiorite||||||
22213|Long Gully Granite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
22213|Long Gully Granite|43060|5|Briefly described|Table 6|||of Almaden Supersuite||||||
22213|Long Gully Granite|43083|4|Described|p252|||Of Almaden Supersuite. I-type. Lithology included.||||||17-JUN-09
22213|Long Gully Granite|43087|2|Defined|p75|Late Carboniferous||Of Almaden Supersuite.||||||29-APR-09
22213|Long Gully Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Long Gully Suite (Almaden Supersuite).||||||15-JUN-06
22213|Long Gully Granite|43254|5|Briefly described|map legend||Late Carboniferous|of Almaden Supersuite.||||||
22213|Long Gully Granite|43625|6|Mentioned|p51|||||||||
22213|Long Gully Granite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Long Gully Suite (Almaden Sup'ste). Med.-gr.slightly to mod'ly porphyritic hornblende-biotite granite+mafic enclaves (to 30cm)common;commonly slightly altered;forms net-veined complexes, 'diorite' in several places; minor Cu mineralisation. I-type||||||07-FEB-11
22213|Long Gully Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Almaden Supersuite.|||Pale grey to pinkish grey, medium-grained, porphyritic hornblende-biotite monzogranite to granodiorite?; commonly slightly altered; forms net-veined complexes with "diorite" in places.|
30426|Long Gully Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite (Almaden Supersuite).||||||15-JUN-06
30426|Long Gully Suite|60425|5|Briefly described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of the Almaden Supersuite. Contains Long Gully Granite. I-type.||||||31-MAR-15
35394|Long Mountain Breccia Member|61392|5|Briefly described|p163, p165 Fig. 1|||A separate unit that forms the lower 300m of the Bromley Hills Formation.||||||07-FEB-11
35394|Long Mountain Breccia Member|63731|5|Briefly described|Map legend||Silurian|Of Bromley Hills Volcanics (Silverwood Group). Polymictic megabreccia containing sedimentary as well as basaltic to andesitic clasts and cross-stratified pebbly arenite.||||||13-DEC-07
35394|Long Mountain Breccia Member|63748|4|Described|p9||Middle Devonian|Of Bromley Hills Formation (Silverwood Group). Thickness 350m. Geol.Prov: Silverwood province. Polymictic megabreccia capped by 60m of cross-stratified pebbly arenite.||||||07-FEB-11
35394|Long Mountain Breccia Member|68679|5|Briefly described|p447|Middle Devonian|Middle Devonian|Silverwood Province. 350m thick.||Basal Bromley Hills Formation.|||Polymict megabreccia containing basaltic to andesitic fragments and various clastic sedimentary blocks (debris flows initiated by catastrophic collapse along the margins of a stratovolcano), capped by 60m of cross-stratified pebbly sandstone.|
32042|Lookerbie Igneous Complex|23799|5|Briefly described|p117|||Of the Monal Suite (Murray et al, 2000, in prep.).  Geological Province: Yarrol Province||||||
32042|Lookerbie Igneous Complex|24491|4|Described|p23|||||||||
32042|Lookerbie Igneous Complex|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRglo].  Tonalite, granodiorite, quartz diorite and andesite.||||||
32042|Lookerbie Igneous Complex|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
32042|Lookerbie Igneous Complex|60282|5|Briefly described|p8|||Of the Rawbelle Batholith.  Diorite and granodiorite.||||||
32042|Lookerbie Igneous Complex|65388|3|Fully described|p294, 35, 237, 238, 295, 298-299,  301|Early Permian|Early Permian|I-type. Cut by mafic dykes. North of Yaparaba Volcanics. May intrude Yaparaba Volcanics. Age revised herein from that used on SCORIA map, on basis of geochemical similarity to Eidsvold Complex. Includes biotite-hornblende tonalite, granodiorite, quartz diorite, diorite and microdiorite dykes. Plutonic rocks commonly quite strongly altered. See also p340, 447.||||||
32042|Lookerbie Igneous Complex|68008|3|Fully described|p334, p339, p419-421|Triassic|Permian|Taylor (1988), while exploring for gold for Placer Exploration in the Rannes beds (now mapped in this area as Yaparaba Volcanics). The unit occurs to the NE of  Mount Lookerbie, after which it is named. Forms a NW-trending unit 6 x 15 km. The type area is the E bank of Grevillea Creek, just downstream from the junction with Saddle Gully at GR263100 72757000, where numerous tors crop out. Generally forms undulating hills with poor outcrop. Geophysics briefly described. Geochemistry described.||||Adjacent to (probably intrudes) Yaparaba Volcanics.|Diorite, gabbro, tonalite, granodiorite and quartz diorite; commonly quite strongly altered; also andesite.|
32042|Lookerbie Igneous Complex|68679|5|Briefly described|p344, p404, p408, p427|Permian|Permian|Auburn Subprovince, New England Orogen. Similar to Eidsvold Complex. Geochemistry briefly described. Probably early Permian on geochemical and structural setting.|||||Biotite-hornblende tonalite, granodiorite, quartz diorite, diorite and microdiorite dykes.|
40580|Loretta Supersequence|62535|5|Briefly described|p672|Statherian|Statherian|Isa Superbasin.|c.1645 Ma.|||||
40580|Loretta Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Tooganinie Formation, Tatoola Sandstone, Amelia Dolostone and upper parts of Mallapunyah Formation.|||
40580|Loretta Supersequence|63866|5|Briefly described|p53-p54, p56-p57, p59|||Isa Superbasin.|||Includes the Tatoolla Sandstone and Lady Loretta Formation.|Equivalent to the Walford Dolomite, Kennedy Siltstone and Magazine Shale. Conformably overlies the Gun Supersequence.||
40580|Loretta Supersequence|65228|4|Described|pp26-29, Figs.11-21.|Statherian|Statherian|At Mount Isa, interpreted as comprising Kennedy Siltstone, Magazine Shale, Leila Sandstone, Myrtle Shale, Emmerugga Dolomite. A karst surface marks the top of this unit. Gamma ray log, lithology and facies detailed.|c.1650 Ma.|||Equates with Walford Dolomite and Lady Loretta Formation.|Mixed succession of carbonates and siliciclastics. Basal conglomerate, interbedded sandstone and siltstone with evaporites, oolitic and stromatolitic carbonates with thin green shales.|
40580|Loretta Supersequence|65337|6|Mentioned|p33 Fig.27.|||||||Overlies Gun Supersequence. Is overlain by River Supersequence.||
40580|Loretta Supersequence|66844|5|Briefly described|p244-246,269|Mesoproterozoic|Paleoproterozoic|Lawn Hill and Gunpowder region. See also reference to Loretta 1.1, p255 fig 7.||Of McNamara Group.|Includes Lady Loretta Formation.|Underlain unconformably by Gun Supersequence.|non-marine and marine siliciclastics.|
40580|Loretta Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.|~1650-1645 Ma.|||Overlies Gun Supersequence. Is overlain by River Supersequence.|Thin-bedded, intraclastic and stromatolitic dolomite, interbeds of dolomitic siltstone and fine-grained sandstone|
40580|Loretta Supersequence|68732|5|Briefly described|p159, p162, p165 Fig.3|||Contains domal, columnar and digitate stromatolites which combine to form bioherms and biostromes. Includes Lady Loretta and Magazine/Kennedy Siltstones.||||||01-DEC-17
40580|Loretta Supersequence|69591|5|Briefly described|p27, p42-43, p46, p54, p108|||Mount Isa Province, Isa Superbasin. Shallow-water carbonate platform deposits. Includes the Lady Loretta Formation.||||Unconformably overlies Gun Supersequence. Is overlain by River Supersequence.||
40580|Loretta Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1650 Ma|||Overlies the Gun Supersequence.|Siltstone, carbonaceous shale and dolomite.|
40580|Loretta Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Paleoproterozic|Paleoproterozic|Kerogens within this unit contain the potential to generate gas and condensate over a large area.||||||
40580|Loretta Supersequence|73144|4|Described|p8-9, p11, p19-20|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains two third order sequences [see article for more detail on third order sequences]. Deposited in shallow marine ram setting with subtidal tempestite cycles (Southgate et al., 2000). Thick carbonate succession. Basal breccia unit sourced from underlying Gun Supersequence. Contains dates of ca 1655 Ma [near the base?] and 1647 +/- 4 Ma [near the top?]. Potential hydrocarbon reservoirs; no potential unconventional hydrocarbon source rocks identified within this supersequence (Gorton and Troup, 2018).|1645-1655 Ma|||Includes Lady Loretta Formation.|Dolomudstone. Includes basal breccia unit.|
32558|Lorray Formation|24488|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32558|Lorray Formation|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPl].  Bryozoan-rich mudstone, fossiliferous siltstone, sandstone, granite-rich, quartz-bearing polymictic conglomerate, and subordinate crinoid-rich limestone.||||||
32558|Lorray Formation|50208|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32558|Lorray Formation|50209|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32558|Lorray Formation|50213|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Bryozoan-rich mudstone, fossiliferous siltstone, sandstone, granite-rich, quartz-bearing polymictic conglomerate and subordinate crinoid-rich limestone.||||||17-MAY-04
32558|Lorray Formation|50317|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Bryozoan-rich mudstone, fossiliferous siltstone, sandstone, granite-rich quartz-bearing polymictic conglomerate, and subordinate crinoid-rich limestone.||||||09-JUN-04
32558|Lorray Formation|60479|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Mudstone, Siltstone, Sandstone, Conglomerate.||||||21-OCT-04
32558|Lorray Formation|60481|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Bryozoan-rich mudstone, fossiliferous siltstone, sandstone, granite-rich, quartz bearing, polymictic conglomerate and subordinate crinoid-rich limestone.||||||
32558|Lorray Formation|60557|4|Described|p19 Fig. 5b, p23|Early Permian|Middle Carboniferous|Dominated by siltstone and sandstone, with local areas of bryozoan mudstone and minor polymictic conglomerate. Conformably to disconformably overlies the Rockhampton Group. Hosts gold and copper mineralisation. See also p20 Fig. 5c.||||||28-MAY-08
32558|Lorray Formation|61035|5|Briefly described|p13|||Lorray Formation supersedes Neerkol Formation. Geological Province: Yarrol Province. Interbedded volcaniclastic sandstone, fine ash-fall tuff and dark siltstone, pebble conglomerate occures sporadically.||||||07-FEB-11
32558|Lorray Formation|61778|6|Mentioned|p241|Late Carboniferous|Early Carboniferous|||||||07-FEB-11
32558|Lorray Formation|64399|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Overlies Rockhmapton Group. Bryozoan-rich mudst., siltst., fossiliferous siltst., sandst., granite-rich, quartz-bearing, polymictic conglomerate, and subordinate crinoid-rich limestone.||||||19-AUG-08
32558|Lorray Formation|64429|6|Mentioned|p17|Late Carboniferous|Early Carboniferous|Part of the Yarrol Block. ||||||
32558|Lorray Formation|65388|4|Described|p74-75; p70 Fig.28; p50, 58, 70|Early Permian|Middle Carboniferous|Rockhampton Subprovince, Yarrol Province. Conformably (gradationally) overlies Rockhampton Group; described by Leitch and others (1994) as Neerkol Formation overlying Campwyn Volcanics. In (thrust?) contact with Shoalwater Formation. Age overlap wth Youlambie Conglomerate. Namurian fossils. May correlate in part with Glenprairie beds. Very thin to very thick-bedded volcaniclastic sandstone and dark siltstone with widespread ash-fall tuff and less common pebble conglomerate on Long Island.||||||08-SEP-14
32558|Lorray Formation|67203|6|Mentioned|p7|Permian|Late Carboniferous|||||||
32558|Lorray Formation|68008|2|Defined|p2,p11,p91, p107-109, p120-123, p131-132|Permian|Late Carboniferous|See also p180-181, p217, p254-255, p261, p359, p366, p481, p483-484, p490, p569, p582-583, p596. Named after Lorray homestead. Combines a number of previously defined units: Neerkol, Branch Creek, Poperima, Rands, Dakiel (in part) and Burnett Formations. The type area is in the Yarrol Syncline near Lorray homestead, where it is 3500-4100m thick. References to type sections for the former constituent units are given. Forms low to moderately hilly topography with prominent strike ridges. Marine shelf deposits: abundant marine macrofossils. Fossil species listed. Overlaps Youlambie Conglomerate in age: discussed. Timing of deformation discussed. Shelly fossils listed. Conformably, locally disconformably, overlies Rockhampton Group. Is intruded by Quarry Gabbro and Kabra Quartz Monzodiorite.||||Is overlain by Yarrol Formation or Youlambie Conglomerate conformably; by Dinner Creek Conglomerate disconformably; by Mount Salmon Volcanics and Dalma Basalt unconformably. See Comments.|Granule to cobble conglomerates; medium- to coarse-grained, lithic to feldspatholithic sandstones; minor fossiliferous fine-grained lithic sandstone, siltstone, dark calcareous mudstone (locally dominant), detrital and fossiliferous limestones.|
32558|Lorray Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Yarrol Province. ||||||
32558|Lorray Formation|68679|5|Briefly described|p308, p312-314, p337-338, p341, p345|Cisuralian|Pennsylvanian|See also p347, p426, p468. Rockhampton Subprovince, Northern Yarrol Province. Combines the Neerkol and Burnett Formations with the Boiling Creek Group (Branch Creek, Poperima, Rands Formations), all of which are thus superseded. A source of sediments for the Moah Creek beds.||||Overlies Rockhampton Group. Is intruded by Kabra Quartz Monzodiorite and Quarry Gabbro.|Mainly sandstone and bryozoan-rich mudstone; characterised by ubiquitous granitic detritus and quartz in conglomerate and sandstone. Also siltstone, limestone and bioclastic limestone. Proportions differ locally.|
32558|Lorray Formation|69952|6|Mentioned|p75|Permian|Late Carboniferous|||||||
32558|Lorray Formation|73450|6|Mentioned|p67|||||||||
33150|Lotus Creek Rhyolite|23042|4|Described|p14,7,8,23,4,7,30,9|Early Permian|Late Carboniferous|Part of the Connors Volcanics.  Underlying unit Connors Volcanics.||||||
33150|Lotus Creek Rhyolite|60475|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich to very crystal rich (feldspar and quartz), generally lithic poor, locally fiamme bearing, rhyolitic ignimbrite.||||||
33150|Lotus Creek Rhyolite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich to very crystal rich, generally lithic poor, locally fiamme bearing, rhyolitic ignimbrite.||||||
33150|Lotus Creek Rhyolite|61035|5|Briefly described|p6|Carboniferous|Carboniferous|Of the Conners Volcanic Group. Age: ~303Ma (Withnall et al., 1998a,b; Hutton et al., 1999). Consists of rhyolitc ignimbrite, and may be an intra-caldera facies. Geological Province: Connors Sudprovince.||||||07-FEB-11
33150|Lotus Creek Rhyolite|65388|4|Described|p98-100,  p90, 99, 85, 86, 90, 92|Early Permian|Late Carboniferous|Of Connors Volcanic Group, Connors Arch. SHRIMP Age: 295 +/-3.4 Ma. Overlain by Leura Volcanics. Relationship to other surrounding units is unclear. Most likely to be faulted. Postdates Burwood Complex. Type section was previously of the Connors Volcanics (Malone and others, 1966, 1969). Mostly comprises massive, grey, crystal-rich, lithic-poor, rhyolitic ignimbrite. See also p94, 95, 103, 106, 110, 447.||||||
33150|Lotus Creek Rhyolite|68679|4|Described|p353, p355-357, p360-361|Asselian|Asselian|Withnall et al. (2009). Occurs W of St. Lawrence. Southern Connors Subprovince. May infill a large cauldron subsidence area. This U-Pb zircon age suggests a hiatus of 15-20 my.|295 +/- 3.4 Ma (SHRIMP: Fanning et al., 2009).|Connors Volcanic Group.||Is overlain by Leura Volcanics.|Massive grey, crystal-rich, lithic-poor, rhyolitic ignimbrite; probably a single, flat-lying sheet. The groundmass is commonly recrystallised.|
33150|Lotus Creek Rhyolite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Ignimbrite.|
39615|Louey Granite|50199|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
39615|Louey Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Foliated to gneissic, medium- to coarse-grained equigranular to coarsely porphyritic biotite granite.|
79427|Lowman Tank Granite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event||Williams Supersuite|||Foliated biotite granite|
79427|Lowman Tank Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Foliated biotite granite.|
79427|Lowman Tank Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Subsurface; shown on map Schematic Diagram.||Williams Supersuite.|||Foliated biotite granite.|05-MAY-16
79427|Lowman Tank Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Foliated biotite granite.
|
79427|Lowman Tank Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Williams Supersuite|||Foliated biotite granite.|20-JAN-22
79427|Lowman Tank Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Williams Supersuite|||Foliated biotite granite.
|
23742|Lubrina Granite|23291|5|Briefly described|p97 Tb. 3.11|Visean|Visean|Of the Newcastle Range I-types. Age: 331Ma. Geological Province: Georgetown Region.||||||08-JUL-15
23742|Lubrina Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 10. I-Type.||||||
23742|Lubrina Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23742|Lubrina Granite|40542|6|Mentioned|p97|||||||||
23742|Lubrina Granite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
23742|Lubrina Granite|43740|4|Described|p17|||||||||
27824|Lucky Creek Metamorphic Group|22533|6|Mentioned|p54,p56||Early Paleozoic|placed in Thalanga Province||||||07-NOV-08
27824|Lucky Creek Metamorphic Group|23032|5|Briefly described|p14|||||||||
27824|Lucky Creek Metamorphic Group|23291|3|Fully described|p35, p82 Tb. 3.6|Ordovician|Cambrian|Geological Province: Georgetown Region.||||||08-JUL-15
27824|Lucky Creek Metamorphic Group|23430|5|Briefly described|p469|||Has not been dated. Text refers to Lucky Creek Metamorphic Group and Lucky Metamorphic Group.||||||
27824|Lucky Creek Metamorphic Group|23431|5|Briefly described|p532|||Thalanga Province||||||
27824|Lucky Creek Metamorphic Group|23453|5|Briefly described|p10 Fig.1|Ordovician|Cambrian|||||||
27824|Lucky Creek Metamorphic Group|23619|4|Described|p35 Table 1||Early Paleozoic|Previously Lucky Creek Formation. Also see p6. Bally Knob Volcanics and McBride Basalt Group - unconformably. Georgetown Province.||||||07-NOV-08
27824|Lucky Creek Metamorphic Group|41675|1|Redefined|p36|Early Paleozoic||Modified name, originally Lucky Creek Formation||||||07-NOV-08
27824|Lucky Creek Metamorphic Group|42054|6|Mentioned|p273|||||||||
27824|Lucky Creek Metamorphic Group|42279|6|Mentioned|Fig.2 P18|||||||||
27824|Lucky Creek Metamorphic Group|42407|5|Briefly described|p33|||Formerly Lucky Creek Formation||||||
27824|Lucky Creek Metamorphic Group|42474|6|Mentioned|p28|||||||||
27824|Lucky Creek Metamorphic Group|42693|5|Briefly described|map legend|Proterozoic|Early Paleozoic|||||||07-NOV-08
27824|Lucky Creek Metamorphic Group|43113|4|Described|Table 1 p21|||of Early Palaeozoic (Ordivician?)||||||
27824|Lucky Creek Metamorphic Group|43213|6|Mentioned|p62|||Georgetown Province. Parts of this unit are lithologically and structurally similar to the Anakie Metamorphic Group. However, other rocks in the area have been correlated with Seventy Mile Range Group.||||||
27824|Lucky Creek Metamorphic Group|43253|5|Briefly described|map legend|Ordovician|Cambrian|||||||
27824|Lucky Creek Metamorphic Group|43259|6|Mentioned|Appendix 1,p4.||Ordovician|Ordovician?.||||||
27824|Lucky Creek Metamorphic Group|43286|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
27824|Lucky Creek Metamorphic Group|65887|5|Briefly described|p40 Fig.1|Ordovician|Cambrian|Presented in figure legend as Lucky Creek/Balcooma Metamorphic Groups.||||||04-JUN-15
27824|Lucky Creek Metamorphic Group|67455|4|Described|p575 Table 1, p576.|Early Ordovician|Late Cambrian|A metavolcanic assemblage. Lucky Creek domain, Greenvale Province. Similar to the Seventy Mile Range Group in the Charters Towers Province. East of the Dido Tonalite.|||Includes Lugano Metamorphics, Eland Metavolcanics, and Paddys Creek Phyllite.||Mafic to silicic volcanic and volcaniclastic rocks.|04-MAY-12
27824|Lucky Creek Metamorphic Group|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.|||Includes Lugano Metamorphics, Eland Metavolcanics and Paddys Creek Phyllite.|||
27824|Lucky Creek Metamorphic Group|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.|||Includes Lugano Metamorphics, Eland Metavolcanics and Paddys Creek Phyllite.|||
27824|Lucky Creek Metamorphic Group|68553|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
27824|Lucky Creek Metamorphic Group|68576|5|Briefly described|Q_11: p33, p35|||Age and relationships uncertain; probably Cambrian or Ordovician; may be correlative  of Seventy Mile Range Group.|||Lugano Metamorphics, Paddys Creek Phyllite, Eland Metavolcanics.|||
27824|Lucky Creek Metamorphic Group|68731|5|Briefly described|p152, p155, p158, p159, p220|Ordovician|Ordovician|Lies east of the Dido Tonalite. Considered to have formed by mafic to silicic volcanism with associated probable marine and volcaniclastic sedimentation. Metamorphic grade decreases from west to east.|||Includes Lugano Metamorphics, Eland Metavolcanics, Paddys Creek Phyllite.|Possible temporal equivalent of the Balcooma Metavolcanic Group and the Mount Windsor Volcanics.||11-MAY-16
27824|Lucky Creek Metamorphic Group|69079|5|Briefly described|p60|Ordovician|Cambrian|Hosts gold mineralisation in quartz veins in the the Lucky Creek Goldfield.|||Lugano Metamorphics, Eland Metavolcanics.|Is intruded by Dido Tonalite.|Includes biotite gneiss, amphibolite, calcareous chlorite-mica schist, marble, metachert.|
27824|Lucky Creek Metamorphic Group|69952|5|Briefly described|p6, p104|||Greenvale Province, Thomson Orogen.|||Includes Lugano Metamorphics.|||
27824|Lucky Creek Metamorphic Group|70749|5|Briefly described|p42-43|Ordovician|Ordovician|Greenvale Province.|||||Mainly felsic metavolcanic and metasedimentary sequences representing back arc basin deposits.|
27824|Lucky Creek Metamorphic Group|71966|6|Mentioned|p990|Ordovician|Ordovician|Geological province: Greenvale Province, Thomson Orogen. ||||||
22223|Lucy Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
22223|Lucy Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
22223|Lucy Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 314. I-Type.||||||
22223|Lucy Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22223|Lucy Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
22223|Lucy Granite|43087|2|Defined|p33|Late Carboniferous||Of Ootann Suite of Richards (1981) and Ootann Supersuite of Champion (1991).||||||
22223|Lucy Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22223|Lucy Granite|43259|4|Described|Appendix 1,p38.||Late Carboniferous|||||||
22223|Lucy Granite|43626|6|Mentioned|p10|||||||||
22223|Lucy Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Medium to coarse-gr., even-gr. (hornblende-) biotite granite; rounded mafic enclaves (most <5cm) common; locally converted to clinopyroxene-bearing endoskarn; minor porphyritic microgranite.||||||07-FEB-11
22223|Lucy Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma, 310 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pink, medium- to fine-grained, moderately porphyritic biotite monzogranite; locally with rare hornblende; with scattered inclusions up to ~1 m across (most < 10 cm).|
23743|Lugano Metamorphics|22844|6|Mentioned|p31|Early Paleozoic|Proterozoic|||||||07-NOV-08
23743|Lugano Metamorphics|23032|4|Described|p14|||||||||
23743|Lugano Metamorphics|23291|4|Described|p35, p82 Tb. 3.6|Ordovician|Cambrian|Intruded by Cockie Springs Tonalite. Parent: Lucky Creek Metamorphic Group. Geological Province: Georgetown Region.||||||08-JUL-15
23743|Lugano Metamorphics|23430|5|Briefly described|p469-470|||Referred to as part of Lucky Creek Metamorphic Group and Lucky Metamorphic Group.||||||07-MAY-15
23743|Lugano Metamorphics|23431|5|Briefly described|p532|||Of Lucky Creek Metamorphic Group. Thalanga Province.||||||
23743|Lugano Metamorphics|23619|4|Described|p35 Table 1|||Intruded by Cockie Spring Tonalite and Dido Tonalite. Also see p6. Of Lucky Creek Metamorphic Group. Georgetown Province.||||||
23743|Lugano Metamorphics|41675|2|Defined|p37|Proterozoic||||||||
23743|Lugano Metamorphics|41916|6|Mentioned|p26|||||||||
23743|Lugano Metamorphics|41975|5|Briefly described|p439|||||||||
23743|Lugano Metamorphics|42054|6|Mentioned|p272|||||||||
23743|Lugano Metamorphics|42279|4|Described|p17|||See also Fig.2||||||
23743|Lugano Metamorphics|42407|5|Briefly described|p33|||Also Fig. 20 p29||||||07-MAY-15
23743|Lugano Metamorphics|42692|5|Briefly described|map legend|Ordovician|Cambrian|||||||
23743|Lugano Metamorphics|42693|5|Briefly described|map legend|Proterozoic|Early Paleozoic|||||||07-NOV-08
23743|Lugano Metamorphics|43113|4|Described|Table 1 p22|||Tentatively early Palaeozoic (possibly Proterozoic). Of Lucky Creek Metamorphic Group.||||||
23743|Lugano Metamorphics|43253|5|Briefly described|map legend|Ordovician|Cambrian|of Lucky Creek Metamorphic Group||||||
23743|Lugano Metamorphics|43286|5|Briefly described|Map Legend|Ordovician|Cambrian|of Lucky Creek Metamorphic Group.||||||
23743|Lugano Metamorphics|43480|6|Mentioned|49||Late Devonian|||||||
23743|Lugano Metamorphics|43664|6|Mentioned|Fig.3,p15|||||||||
23743|Lugano Metamorphics|43716|6|Mentioned|p116|||||||||
23743|Lugano Metamorphics|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
23743|Lugano Metamorphics|67455|4|Described|p575 Table 1, p576, pp583-584, p586.|Ordovician|Cambrian|Lucky Creek domain, Greenvale Province. Metamorphic grade decreases from amphibolite facies eastwards. An overall extensional backarc setting, to the west of a subduction-related arc, is inferred. Also mis-spelled as Lugarno Metamorphics on p576 Fig.2.||||||04-MAY-12
23743|Lugano Metamorphics|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province. Two subordinate facies are mapped separately: amphibolite, local relict pillow lavas; and biotite gneiss and schist grading to nebulitic and agmatitic migmatite, foliated biotite granite containing abundant xenoliths and schlieren, local tourmaline-muscovite pegmatite veins.||Unit in Lucky Creek Metamorphic Group.|||Biotite gneiss, mica schist, quartzite, leucogneiss, laminated amphibolite and minor marble.|
23743|Lugano Metamorphics|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province. Two subordinate facies are mapped separately: amphibolite, local relict pillow lavas; and biotite gneiss and schist grading to nebulitic and agmatitic migmatite, foliated biotite granite containing abundant xenoliths and schlieren, local tourmaline-muscovite pegmatite veins.||Unit in Lucky Creek Metamorphic Group.|||Biotite gneiss, mica schist, quartzite, leucogneiss, laminated amphibolite and minor marble.|
23743|Lugano Metamorphics|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Thalanga Province. Four facies are mapped separately.|||||Biotite gneiss and schist grading to nebulitic and agmatitic migmatite; amphibolite with local relict pillow lavas; quartzite (locally with kyanite); biotite gneiss, mica schist, quartzite, leucogneiss, laminated amphibolite and minor marble.|
23743|Lugano Metamorphics|68576|5|Briefly described|Q_11: p33|||Age and relationships uncertain; probably Cambrian or Ordovician; may be correlative  of Seventy Mile Range Group.||Lucky Creek Metamorphic Group.||||
23743|Lugano Metamorphics|68731|5|Briefly described|p151 Fig 3.51, p153 Fig 3.52, p155, p158|Ordovician|Cambrian|Amphibolite is mainly fine grained and consists of hornblende, plagioclase and epidote at lower metamorphic grade. Detailed lithology discussed.||Of the Lucky Creek Metamorphic Group.||Intruded by the Cockie Spring Tonalite. Underlain by the Eland Metavolcanics.|Comprises abundant amphibolite in the central part of the outcrop area and more common schist, leucogneiss and quartzite in the east and west.|
23743|Lugano Metamorphics|69079|5|Briefly described|p60|||Hosts gold mineralisation in quartz veins in the the Lucky Creek Goldfield.||Lucky Creek Metamorphic Group||Is intruded by Dido Tonalite.||
23743|Lugano Metamorphics|69952|4|Described|p2 Tb.i, p6, p104-107|||NW of Charters Towers; Greenvale Province, Thomson Orogen. Has undergone three phases of deformation. SHRIMP U-Pb zircon: a "reconnaissance age of uncertain significance". Being within error of the age of the Dido Tonalite, there is the possibility that the latter intruded its own volcanic pile (represented by the Lugano Metamorphics).|434.0 +/- 5.0 Ma (Cross et al., 2015).|Unit in Lucky Creek Metamorphic Group.||Is intruded by Dido Tonalite and the undated Cockie Springs Tonalite.|Amphibolite (preserving primary relict pillow lavas, hyaloclastites and amygdales), meta-rhyolite, and leucocratic gneissic rocks that were possibly volcaniclastic metasedimentary rocks. Includes sillimanite-biotite-feldspar-quartz schist.|
23743|Lugano Metamorphics|72297|5|Briefly described|p721|||A potential source of kyanite at Dido Hill, SE of Conjuboy homestead.|||||Quartzite.|
31681|Lukinville Granodiorite|23420|4|Described|p 152 table 4.8||Early Devonian|In the Lukinville Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group||||||
31681|Lukinville Granodiorite|23496|5|Briefly described|Table 2, p37|Devonian|Silurian|of Lukinville Suite, Kintore Supersuite.||||||
31681|Lukinville Granodiorite|43596|4|Described|p30, p26 Tb. 2, p29 Tb. 3|||Of Lukinville Suite (Kintore Supersuite). Intrudes Daintree and Arakara Gneisses, and Jedda and Saraga Schists. Pale to med.grey. med.gr, even-gr. to slightly porphyritic (garnet-sillimanite) biotite-muscovite granodiorite, locally with sparse muscovite.||||||07-APR-15
31681|Lukinville Granodiorite|69592|5|Briefly described|p282, p286-288 Figs.4.80-81,84|||Southern Cape York Peninsula Batholith. Geochemistry briefly described.||Kintore Supersuite.|||Extensively deformed granitoid. S-type.|
31681|Lukinville Granodiorite|70207|4|Described|p4, p11, p72-80|Early Devonian|Early Devonian|Southern Cape York Peninsula Batholith. Similar age to the ~410-395 Ma granitoids of the Pama Igneous Association to the north, in the Coen region.|412.1 +/- 4.0 Ma (Kositcin et al., 2015).|Lukinville Suite.||Intrudes Yambo Metamorphic Group.|S-type. Pale grey, medium-grained, slightly porphyritic muscovite-biotite granodiorite. Quartz forms scattered, anhedral phenocrysts or aggregates as well as more abundant groundmass grains.|
31681|Lukinville Granodiorite|70345|6|Mentioned|p3|Devonian|Devonian|Of the Pama Igneous Association.||||||
31681|Lukinville Granodiorite|70673|6|Mentioned|p7|Devonian|Devonian|||||||
31681|Lukinville Granodiorite|71592|5|Briefly described|Appendix A.|||Palma Igneous Province.|412+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
29748|Lukinville Suite|23420|4|Described|p 152 table 4.8||Early Devonian|Also see p 147 table 4.6. In the Kintore Supersuite.||||||
29748|Lukinville Suite|23496|5|Briefly described|Table 2, p37|Devonian|Silurian|of Kintore Supersuite.||||||
29748|Lukinville Suite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
29748|Lukinville Suite|43596|4|Described|p29-30, p26 Tb. 2|||Of Kintore Supersuite.  Contains Fenhill Granite, and Lukinville and Rocky King Granodiorites.||||||27-JAN-09
29748|Lukinville Suite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kintore Supersuite||||||24-JAN-05
29748|Lukinville Suite|70207|5|Briefly described|p73|Devonian|Devonian|Southern part of the Cape York Peninsula Batholith. Unit in Pama Igneous Association.||Kintore Supersuite.|Lukinville Granodiorite.|||
30123|Lulu Pocket Igneous Complex|22847|3|Fully described|p 57|Permian|Carboniferous|||||||
30123|Lulu Pocket Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
30123|Lulu Pocket Igneous Complex|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30123|Lulu Pocket Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 200. I-Type.||||||
30123|Lulu Pocket Igneous Complex|43093|4|Described|Appendix 1|Permian|Carboniferous|Reserved as Lulu Pocket Granodiorite||||||
30123|Lulu Pocket Igneous Complex|43259|4|Described|Appendix 1,p29.|Permian|Carboniferous|||||||
30123|Lulu Pocket Igneous Complex|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30123|Lulu Pocket Igneous Complex|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Suite.||||
22227|Lumma Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Djungan Volcanic Subgroup of Featherbed Volcanic Group.||||||
22227|Lumma Rhyolite|23430|6|Mentioned|p498|||Of Featherbed Volcanic Group.||||||
22227|Lumma Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Of Djungan Volcanic Subgroup and Lags Supersuite.||||||
22227|Lumma Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V107. A-Type.||||||
22227|Lumma Rhyolite|23616|5|Briefly described|Table 3 p46|||Rb-Sr total rock age 281+/-2 Ma. Of Djungan Volcanic Subgroup/Featherbed Volcanic Group.||||||
22227|Lumma Rhyolite|23713|5|Briefly described|p23|||Age: 281+/-2 Ma (Rb-Sr isotope). Of Featherbed Volcanic Group. Maximum thickness: 300 m.||||||
22227|Lumma Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group.||||||01-APR-15
22227|Lumma Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group). Intensely welded rhyolitic ignimbrite with rare garnet. Age: 281+/-2Ma.||||||01-APR-15
22227|Lumma Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Djungan Subgroup. Age 281+/-2 Ma.||||||
22227|Lumma Rhyolite|43259|4|Described|Appendix 1,p11.||Early Permian|of Djungan Volcanic Subgroup. Age is 281+/-2 Ma.||||||
22227|Lumma Rhyolite|43285|5|Briefly described|Map Legend||Permian|of Djungan Volcanic Subgroup.||||||
22227|Lumma Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
22227|Lumma Rhyolite|43625|5|Briefly described|p38|||Age: 281+/-2 Ma||||||
22227|Lumma Rhyolite|43626|2|Defined|p66||Early Permian|Rb-Sr dating: 281+/-2 Ma||||||
22227|Lumma Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
22227|Lumma Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 281 +/- 2 Ma (Rb, Sr). Of Djungan Volcanic Group (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
22227|Lumma Rhyolite|60425|5|Briefly described|p46 Tb. 3|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
22227|Lumma Rhyolite|62523|5|Briefly described|Map legend at p3-4, p19 Tb. 2|Early Permian|Early Permian|In the Featherbed Cauldron. Medium to very dark grey or greenish-grey, intensely welded, lithics-free to very lithics-poor, very crystal-rich to crystal-rich rhyolitic ignimbrite with rare garnet, and pale 'coarse-porphyritic' pumice clasts. Age:281+/-2Ma||||||07-FEB-11
22227|Lumma Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Djungan Volcanic Subgroup.||Overlies Lightning Creek Rhyolite.|Medium to very dark grey or greenish grey, intensely welded, lithics-free to very lithics-poor, very crystal-rich to crystal-rich rhyolitic ignimbrite, with rare garnet and pale grey coarsely porphyritic 'pumice' clasts to 20 cm.|
22227|Lumma Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Included in Lags Supersuite.|281 Ma.|Featherbed Volcanic Group.|||A-type.|
25185|Lunch Creek Gabbro|22522|6|Mentioned|Fig2p332,Fig3p333|||||||||
25185|Lunch Creek Gabbro|23071|5|Briefly described|p760|Statherian|Statherian|||||||
25185|Lunch Creek Gabbro|23192|6|Mentioned|Fig.2|||||||||
25185|Lunch Creek Gabbro|23324|5|Briefly described|p468 Fig.1|||Gabbro and metagabbro.||||||07-FEB-07
25185|Lunch Creek Gabbro|23396|6|Mentioned|p423 Fig.17|||||||||
25185|Lunch Creek Gabbro|23397|6|Mentioned|p464 Fig.3|||||||||
25185|Lunch Creek Gabbro|23959|6|Mentioned|p1166|||Intrudes the Corella Formation.  Geological Province: Mount Isa Inlier.||||||
25185|Lunch Creek Gabbro|23967|6|Mentioned|p1331 Fig.1|||||||||
25185|Lunch Creek Gabbro|24255|5|Briefly described|p32 Fig.1|||Geological Province: Eastern Succession, Mount Isa Block.||||||
25185|Lunch Creek Gabbro|24256|6|Mentioned|p50 Fig.2|||Geological Province: Mount Isa Block.||||||
25185|Lunch Creek Gabbro|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
25185|Lunch Creek Gabbro|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
25185|Lunch Creek Gabbro|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
25185|Lunch Creek Gabbro|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25185|Lunch Creek Gabbro|30531|6|Mentioned|p20|||Also mention P22||||||
25185|Lunch Creek Gabbro|30601|5|Briefly described|p418|||See also P419||||||
25185|Lunch Creek Gabbro|32660|5|Briefly described|Table 5|||||||||
25185|Lunch Creek Gabbro|33900|6|Mentioned|p24|||||||||
25185|Lunch Creek Gabbro|35000|6|Mentioned|p137|||||||||
25185|Lunch Creek Gabbro|35074|6|Mentioned|Fig.2|||||||||
25185|Lunch Creek Gabbro|35167|2|Defined|p154|Late Precambrian|Late Precambrian|||||||
25185|Lunch Creek Gabbro|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
25185|Lunch Creek Gabbro|37462|4|Described|Table4.VII|||||||||
25185|Lunch Creek Gabbro|37568|6|Mentioned|p85|||||||||
25185|Lunch Creek Gabbro|38350|6|Mentioned|p19|||||||||
25185|Lunch Creek Gabbro|39049|4|Described|p842|||||||||
25185|Lunch Creek Gabbro|39445|6|Mentioned|p43|||1740 Ma. See also Table 2||||||
25185|Lunch Creek Gabbro|39622|6|Mentioned|p27|||||||||
25185|Lunch Creek Gabbro|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25185|Lunch Creek Gabbro|39937|5|Briefly described|p84|||||||||
25185|Lunch Creek Gabbro|40840|6|Mentioned|Map legend|||||||||
25185|Lunch Creek Gabbro|41125|6|Mentioned|p45|||||||||
25185|Lunch Creek Gabbro|41465|5|Briefly described|p11|||||||||
25185|Lunch Creek Gabbro|41594|5|Briefly described|p74|||||||||
25185|Lunch Creek Gabbro|41957|5|Briefly described|p66|||||||||
25185|Lunch Creek Gabbro|41978|6|Mentioned|p502|||||||||
25185|Lunch Creek Gabbro|41979|6|Mentioned|Fig.2 P512|||||||||
25185|Lunch Creek Gabbro|42201|6|Mentioned|p292|||||||||
25185|Lunch Creek Gabbro|42365|5|Briefly described|Fig.3 P258|||Also P264, Fig.15||||||
25185|Lunch Creek Gabbro|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1740ma. Gabbro, dolerite.||||||09-FEB-09
25185|Lunch Creek Gabbro|42781|5|Briefly described|Fig.4 P429|||||||||
25185|Lunch Creek Gabbro|43615|6|Mentioned|p14|||1740+/-24 Ma||||||
25185|Lunch Creek Gabbro|45161|6|Mentioned|p32|||||||||
25185|Lunch Creek Gabbro|45166|5|Briefly described|p20|||||||||
25185|Lunch Creek Gabbro|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25185|Lunch Creek Gabbro|46843|6|Mentioned|Fig.2|||||||||
25185|Lunch Creek Gabbro|46976|6|Mentioned|p97|||||||||
25185|Lunch Creek Gabbro|49009|6|Mentioned|p31|||||||||
25185|Lunch Creek Gabbro|49041|5|Briefly described|Table 2|||||||||
25185|Lunch Creek Gabbro|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.  ||||||
25185|Lunch Creek Gabbro|50332|5|Briefly described|p19|Proterozoic|Proterozoic|Of the Burstall Suite. Intrudes the Corella Formation and forms vein complexes in the Burstall Granite. Outcrops in the Wonga Subprovince.||||||07-FEB-11
25185|Lunch Creek Gabbro|50536|5|Briefly described|p6.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite. Age: 1740 +/- 24Ma (U-Pb).||||||07-NOV-08
25185|Lunch Creek Gabbro|61924|5|Briefly described|p44|||||||||
25185|Lunch Creek Gabbro|61963|5|Briefly described|p770 Fig. 1|||||||||
25185|Lunch Creek Gabbro|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks.||||||
25185|Lunch Creek Gabbro|65396|6|Mentioned|p53, p78|||Mount Isa Block.|c.1.74 Ga.|||||
25185|Lunch Creek Gabbro|65505|6|Mentioned|9976, Fig 1-2,7|Proterozoic|Proterozoic.|Of the Burstall Suite. Co-magmatic with Burstall Granite. Age: 1739 +/- 3 Ma.||||||
25185|Lunch Creek Gabbro|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Mount Isa Province, with correlatives in the Eastern Gawler Province. Produced in the Lunch Creek Event, ME 11 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1750 Ma.|||||
25185|Lunch Creek Gabbro|67323|4|Described|GIS attrib tbl, Solid Geology Map, p15|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier. Wonga/Burstall Igneous Event. Two other, similar, ages are given.|1739 +/- 3 Ma.|Wonga Suite, Burstall Suite.||Time-equivalent to the Wonga Suite.|Olivine-pyroxene gabbro, biotite diorite, hybrid diorite and tonalite.|
25185|Lunch Creek Gabbro|68542|6|Mentioned|p20 fig 6|||||||||
25185|Lunch Creek Gabbro|68576|6|Mentioned|Q_2: p20|||Mary Kathleen area.||||||
25185|Lunch Creek Gabbro|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|Igneous crystallisation ages.|1737 +/- 3; 1739 +/- 3 Ma|||||
25185|Lunch Creek Gabbro|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1739 +/- 3 Ma.|||||
25185|Lunch Creek Gabbro|69591|5|Briefly described|p60||||1739 +/- 3 Ma (Neumann et al., 2009).|Burstall Suite.|||Olivine-pyroxene gabbro, biotite diorite, hybrid diorite and tonalite.|
25185|Lunch Creek Gabbro|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Olivine-pyroxene gabbro, biotite diorite, hybrid diorite and tonalite.|
25185|Lunch Creek Gabbro|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Olivine-pyroxene gabbro, biotite diorite, hybrid diorite and tonalite.|
25185|Lunch Creek Gabbro|71592|5|Briefly described|Appendix A.|||Kalkadoon-Leichhardt Domain, Mount Isa Orogen.|1739+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro.|
25185|Lunch Creek Gabbro|72799|6|Mentioned|p1, p19, p38, p50, p56|Statherian|Statherian|Geochron is emplacement age from Neumann et al. (2009). Forms a net-veined complex with the Burstall Granite.|1739 +/- 3 Ma|Burstall Suite[?]||Coeval with Burstall Granite and Wimberu Granite.||
25185|Lunch Creek Gabbro|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb TIMS age of 1740 +/- 24 Ma reported by Page (1983). U-Pb SHRIMP age of 1739 +/- 3 Ma reported by Neumann et al. (2009).|1740 +/- 20 Ma, 1739 +/- 3 Ma|||||
25185|Lunch Creek Gabbro|73553|4|Described|p3, p8, p83, p135-138, p141-142,|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. First mapped on MARRABA by Derrick et al., (1977c). Detailed descriptions provided by Derrick et al., (1971; 1978;1980), and Blake (1981, 1987). Relatively well exposed. Close spatial association and complex contact with Burstall Granite, suggested that the granite intrudes the gabbro. Described with the Burstall Granite as forming a shallowly dipping, thick composite sill. Moderate magnetic response with magnetic striping in detail. Dull green to maroon tones on radiometric images. See also p144-146, p163-164, p173, p177-178, p182, p185, p187-197, p224, p230-231, p266.|1740+/-24 Ma TIMS, 1739+/-3 Ma U-Pb SHRIMP|Burstall Suite||Intrudes Corella Formation, intruded by Lakeview Dolerite|Coarse- to medium-grained, sub-ophitic pyroxene gabbro, containing augite, hypersthene, zoned plagioclase, poikiolitic biotite. Also contains contaminated (hybrid) domains near contacts, tonalite, very coarse-grained pegmatoidal patches.|03-FEB-23
27293|Lyall Formation|22800|5|Briefly described|Fig.14 p592||Visean|||||||
27293|Lyall Formation|23032|4|Described|p36,37|Visean|Visean|||||||
27293|Lyall Formation|23422|6|Mentioned|p181|||||||||
27293|Lyall Formation|23424|4|Described|Table 8.1 Fig 8.4 p338.||Visean|Age: Early Carboniferous (Visean); palynomorphs. Intruded by Carboniferous granites and rhyolite plugs overlain by Wade beds and tertiary basalt and sediments. Parent Clarke River Group, Geological Province Clarke River Basin. Maximum thickness ~1000 m.||||||21-JUN-13
27293|Lyall Formation|23430|4|Described|Plate 14.11 + p509||Carboniferous|Of Clarke River Group. Camel Creek Subprovince. Clarke River Basin Province.||||||
27293|Lyall Formation|23431|5|Briefly described|p542|||Of Clarke River Group.||||||
27293|Lyall Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Clarke River Group.||||||
27293|Lyall Formation|23893|6|Mentioned|p18|||Geological Province: Clarke River Basin.||||||
27293|Lyall Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Visean|Tournaisian|Of the Clarke River Group. Overlies the Ruxton Formation and the Venetia Formation. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
27293|Lyall Formation|24613|5|Briefly described|p94|||Of the Clarke River Group. Lyall was misspelt as Lyell.||||||07-FEB-11
27293|Lyall Formation|24614|5|Briefly described|p191 Fig. 1|||Of the Clarke River Group. Geological Province: Clarke River Basin.||||||07-FEB-11
27293|Lyall Formation|40675|6|Mentioned|Table 4A|||||||||
27293|Lyall Formation|40943|2|Defined|p52|Late Carboniferous|late Visean|Late Visean to Late Carboniferous. See P52 or 54||||||
27293|Lyall Formation|40954|6|Mentioned|p132|||||||||
27293|Lyall Formation|41260|3|Fully described|p23|||See also P181||||||
27293|Lyall Formation|41735|6|Mentioned|p285|||||||||
27293|Lyall Formation|41739|6|Mentioned|p305|||||||||
27293|Lyall Formation|41776|4|Described|p527|||||||||
27293|Lyall Formation|41823|5|Briefly described|p162|||||||||
27293|Lyall Formation|41824|6|Mentioned|p201|||||||||
27293|Lyall Formation|41916|6|Mentioned|p33|||||||||
27293|Lyall Formation|42692|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27293|Lyall Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
27293|Lyall Formation|42933|3|Fully described|p210|||Of Clarke River Group. See also p174.||||||04-FEB-08
27293|Lyall Formation|43095|5|Briefly described|p65|||||||||
27293|Lyall Formation|43259|4|Described|Appendix 1,p5.||Early Carboniferous|of Clarke River Group. Age Early Carboniferous?||||||21-JUN-13
27293|Lyall Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Clarke River Group.||||||
27293|Lyall Formation|67402|4|Described|p239, p244, p245 fig BND/CLR3|Visean|Visean|Clarke River Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under alluvial fan, alluvial plain or lacustrine conditions. Maximum thickness of 1000m. Misspelt as the Lyell Formation on p245. ||Clarke River Group||Overlies the Venetia and Ruxton Formations.|Volcano-lithic sandstone, conglomerate, mudstone, tuffaceous siltstone and impure limestone. Includes rhyolitic ignimbrites.|
27293|Lyall Formation|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|Includes Meath Rhyolite Member.||Green to purple, volcanolithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone.|
27293|Lyall Formation|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|Includes Furry Hoop, and Meath Rhyolite, Members.||Green to purple volcanilithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone; rhyolitic ignimbrite and spherulitic rhyolite.|
27293|Lyall Formation|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|Includes Furry Hoop, and Meath Rhyolite, Members.||Green to purple volcanilithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone; rhyolitic ignimbrite and spherulitic rhyolite.|
27293|Lyall Formation|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|Includes Meath Rhyolite Member.||Green to purple, volcanolithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone.|
27293|Lyall Formation|68478|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|The 2 facies are mapped separately. Clarke River Basin. May include equivalents of the Meath Rhyolite Member.||Of the Clarke River Group.||Conformably underlain by the Venetia Formation.|Green to purple, volcanolithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone; unassigned volcaniclastic rocks (including ignimbrite) and spherulitic rhyolite.|
27293|Lyall Formation|68479|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|The 2 facies are mapped separately. Clarke River Basin. May include some equivalents of the Meath Rhyolite Member.||Of the Clarke River Group.||Conformably underlain by the Venetia Formation.|Green to purple, volcanolithic sandstone, conglomerate, siltstone, shale (commonly calcareous), tuff and minor impure limestone; unassigned volcaniclastic rocks (including ignimbrite) and spherulitic rhyolite.|
27293|Lyall Formation|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
27293|Lyall Formation|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province.||Clarke River Group.|Meath Rhyolite Member.|||
27293|Lyall Formation|69592|4|Described|p274-276|Visean|Visean|Clarke River Basin. Most extensively distributed part of the Group. Locally >1km thick. Contemporaneous with Harry Creek Formation, as well as onset of extensive volcanism throughout northern QLD. Alluvial plain sediments.||Uppermost Clarke River Group.|Meath Rhyolite Member.|Conformably overlies Venetia Formation.|Variably pebbly, volcanilithic sandstone, and pebble to boulder conglomerate interlayered with micaceous siltstone. Has an interval of ignimbrite interlayered with sandstone near the middle of the Formation.|
27293|Lyall Formation|69593|5|Briefly described|p495-496|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.||Clarke River Group.|Meath Rhyolite Member.|||
32138|Lyndale Diorite|23037|5|Briefly described|p73|Permian|Carboniferous|Intrudes the Torsdale Volcanics and Glenleigh Granite.||||||
32138|Lyndale Diorite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgld].  Greenish-grey, fine- to medium-grained hornblende diorite.||||||
32138|Lyndale Diorite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Greenish-grey, fine- to medium-grained hornblende diorite.||||||
32138|Lyndale Diorite|65388|3|Fully described|p265, p236 Fig. 81, p237, 238, 245|Early Permian|Late Carboniferous|Intrudes along the contact between the Torsdale Volcanics and the Glenleigh Granite. Similar to Boam Creek Quartz Monzodiorite to south. Age tentative. May be Early Carboniferous. Fractured greenish-grey, medium to fine grained, two-pyroxene diorite. ||||||
32138|Lyndale Diorite|68679|5|Briefly described|p407|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes along contact between Torsdale Volcanics and Glenleigh Granite.|Greenish-grey, medium- to fine-grained two-pyroxene diorite.|
39611|Lyndbrook Complex|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||||
39611|Lyndbrook Complex|68330|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Foliated biotite and muscovite-biotite granitoid, commonly with streaky layering and schlieren; locally garnetiferous; muscovite and/or biotite leucogranitoid and pegmatite; sillimanite-biotite schist, gneiss, migmatite and rare amphibolite.|
39611|Lyndbrook Complex|68331|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Foliated biotite and muscovite-biotite granitoid, commonly with streaky layering and schlieren; locally garnetiferous; muscovite and/or biotite leucogranitoid and pegmatite; sillimanite-biotite schist, gneiss, migmatite and rare amphibolite.|
39611|Lyndbrook Complex|68405|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Etheridge Province. Includes altered foliated biotite and muscovite-biotite granitoid, commonly with streaky layering and schlieren, garnetiferous; muscovite and/or biotite leucogranitoid and pegmatite; silimanite-biotite schist, gneiss, migmatite and rare amphibolite.||||Overlies Einasleigh Metamorphics.|Foliated biotite and muscovite-biotite granitoid, commonly with streaky layering and schlieren, locally garnetiferous; muscovite and/or biotite leucogranitoid and pegmatite; silimanite-biotite schist, gneiss, migmatite and rare amphibolite.|
39611|Lyndbrook Complex|69591|5|Briefly described|p61, p65, p83-84|||Withnall et al. (2002). Lyndbrook area. These rocks are layered migmatites grading into nebulitic granitoids with abundant schlieren, of the Einasleigh Metamorphics. Metamorphosed at 1620 Ma and ~1595 Ma.|~1560 Ma (SHRIMP: Fanning, unpub.).|||Intrudes McDevitt Metamorphics. Equivalent to older parts of Forsayth Supersuite.|Nebulitic granitoid and migmatite.|
39611|Lyndbrook Complex|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1562+/-8.8 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
39610|Lynwater Complex|50200|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
39610|Lynwater Complex|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
39610|Lynwater Complex|67455|4|Described|p573, pp575-577, p583. |Early Ordovician|Early Ordovician|Western Greenvale Province. Syntectonic intrusions form part of the basement. Deformed plutonic rocks have a steeply-dipping, north-striking foliation. Ages are U-Pb SHRIMP of  magmatic zircon, giving intrusive ages from two samples.|486 +/- 5 Ma and 477 +/- 6 Ma (U-Pb zircon).|||Intrudes Oasis Metamorphics.|Hornblende-bearing and two-mica granitoids (tonalite, granodiorite and granite) grading into orthogneiss.|05-MAY-15
39610|Lynwater Complex|67848|5|Briefly described|p4.|Early Ordovician|Early Ordovician|Greenvale Province. Granodioritic.||||||
39610|Lynwater Complex|68336|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Cape River Province.|||||Biotite, muscovite-biotite and muscovite orthogneiss (deformed granitoid) and strongly foliated leucocratic granite; screens of amphibolite and some paragneiss; cut by later leucogranite and pegmatite veins.|
39610|Lynwater Complex|68341|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Cape River Province.|||||Biotite, muscovite-biotite and muscovite orthogneiss (deformed granitoid) and strongly foliated leucocratic granite; screens of amphibolite and some paragneiss; cut by later leucogranite and pegmatite veins.|
39610|Lynwater Complex|68344|5|Briefly described|Map legend.||Neoproterozoic|Cape River Province. Five facies are mapped separately. Age min: Early Paleozoic?|||||Biotite orthogneiss and schist; strongly foliated leucocratic granite; hornblende-biotite orthogneiss; foliated biotite granite or granodiorite; similar but nebulitic with biotite-rich schlieren.|11-MAY-15
39610|Lynwater Complex|68346|5|Briefly described|Map legend.||Neoproterozoic|Age min: Early Paleozoic?|||||Biotite, muscovite-biotite and muscovite orthogneiss (deformed granitoid) and strongly foliated leucocratic granite; screens of amphibolite and some paragneiss; cut by later leucogranite and pegmatite veins.|11-MAY-15
39610|Lynwater Complex|68410|5|Briefly described|Map Legend|Paleozoic|Neoproterozoic|Early Paleozoic ? minimum age. Shown as older than the Delamerian Orogeny (ca. 500 Ma)and younger than D3 (c. 970 Ma?).|~ 970-500 Ma||||Biotite, muscovite-biotite and muscovite orthogneiss (deformed granitoid) and strongly foliated leucocratic granite; screens of amphibolite and some paragneiss; cut by later leucogranite and pegmatite veins.|
39610|Lynwater Complex|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Brittany, Chipley, Columbia Creek (part), Hogsflesh and Lavery Creek Supersuites; Schreibers and Sunburst Suites; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
39610|Lynwater Complex|68576|5|Briefly described|Q_11: p32-33|Ordovician|Early Ordovician||||||Includes granitoids.|
39610|Lynwater Complex|68731|5|Briefly described|p122 Fig 3.10, p147, p152, p159, p220|Early Ordovician|Early Ordovician|Greenvale Province. Ages determined from zoned magmatic zircon grains by Fergusson et al. (2007). Suggested that this complex is not part of the Einasleigh Metamorphics as originally thought by Withnall (1989) and Withnall et al. (1997).|486 +/- 5 Ma; 477 +/- 6 Ma |||Intrudes the Oasis Metamorphics.|Comprises mainly orthogneiss and schist of tonalitic to granodioritic composition.|11-MAY-16
39610|Lynwater Complex|69952|5|Briefly described|p62|Ordovician|Ordovician|Zoned magmatic zircon grains were dated at 486 +/- 5 Ma and 477 +/- 6 Ma (Fergusson et al., 2007).||||Intrudes Oasis Metamorphics.|Orthogneisses.|
39610|Lynwater Complex|70744|5|Briefly described|p939, p947|||Greenvale Province. Some sediment derived from Mesoproterozoic rocks. U-Pb zircon age of peak metamorphism and igneous activity by Fergusson et al. (2007).|c.485 Ma (estimated from Fig.7).|||||
39610|Lynwater Complex|70749|5|Briefly described|p43|Ordovician|Cambrian|Greenvale Province.|486 +/- 4 Ma; 477 +/- 6 Ma.|||||
39610|Lynwater Complex|71966|6|Mentioned|p989-990|Early Ordovician|Early Ordovician|Geological province: Greenvale Province, Thomson Orogen. |477+\-6 Ma|||||
39610|Lynwater Complex|73425|5|Briefly described|p15-16|Early Ordovician|Early Ordovician|Greenvale Province, Thomson Orogen.|c.485-475 Ma (Fergusson et al., 2007).|||||
78846|MacAlister seam package|65096|6|Mentioned|p372, p376|Middle Jurassic|Middle Jurassic|[informal 'sequence stratigraphy' unit] See also fig.2, p370. Difficult to distinguish from Wambo and Kogan seam packages on basis of wireline logs.||Said to be of the Juandah Coal Measures sequence.||Between overlying Kogan and underlying Wambo seam packages.||
23745|MacCallor Microgranodiorite|23291|5|Briefly described|p97 Tb. 3.11|Carboniferous|Carboniferous|Of the Newcastle Range I-types. Geological Province: Georgetown Region.||||||28-MAY-15
23745|MacCallor Microgranodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 24.||||||
23745|MacCallor Microgranodiorite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23745|MacCallor Microgranodiorite|40542|6|Mentioned|p97|||||||||
23745|MacCallor Microgranodiorite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
23745|MacCallor Microgranodiorite|43740|4|Described|p16|||||||||
23745|MacCallor Microgranodiorite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
23745|MacCallor Microgranodiorite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
23745|MacCallor Microgranodiorite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Brown, moderately to abundantly porphyritic microgranodiorite containing quartz phenocrysts and moderately abundant chlorite.|
23745|MacCallor Microgranodiorite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Brown, moderately to abundantly porphyritic microgranodiorite containing quartz phenocrysts and moderately abundant chlorite.|
34980|Macarthur Coal Group|23034|6|Mentioned|23|||||||||
27947|Macartneys Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Slightly porphyritic garnet-biotite granite with metasedimentry xenoliths and graphitic inclusions near margins.||||||02-JUL-04
27947|Macartneys Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27947|Macartneys Granite|23430|6|Mentioned|p456.|||||||||
27947|Macartneys Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 804. S-Type.||||||
27947|Macartneys Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
27947|Macartneys Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27947|Macartneys Granite|40659|6|Mentioned|p250|||||||||
27947|Macartneys Granite|40860|6|Mentioned|Fig.2|||||||||
27947|Macartneys Granite|40954|6|Mentioned|p133|||||||||
27947|Macartneys Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
27947|Macartneys Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
27947|Macartneys Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Slightly porphyritic (muscovite-) biotite-garnet granite with abundant metasedimentary, generally carbonaceous, xenoliths and graphite inclusions near margins.|
27947|Macartneys Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Slightly porphyritic (muscovite-) biotite-garnet granite with abundant metasedimentary, generally carbonaceous, xenoliths and graphite inclusions near margins.|
27947|Macartneys Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Coarse biotite granite with trace secondary muscovite; contains garnet. Abundant enclaves and disseminated graphite, especially near the roof of the pluton.|
27947|Macartneys Granite|73642|5|Briefly described|p3 Fig.2, p4-5, p6 Fig.4, p8, p10, p13|Calymmian|Calymmian|Georgetown Inlier. S-type. See also p9 Tb.3. Also referred to as Macartneys granite p8.|1562+/-10 Ma|Esmeralda Supersuite|||Garnet-biotite granite.|
23746|Macauley Creek Granite|23422|5|Briefly described|p181, p217 Table 6.11|Carboniferous|Carboniferous|Of Oweenee Supersuite.||||||
23746|Macauley Creek Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23746|Macauley Creek Granite|23893|5|Briefly described|p19|Early Carboniferous|Early Carboniferous|Geological Province: Oweenee Batholith.||||||15-MAY-15
23746|Macauley Creek Granite|24613|6|Mentioned|p109|Carboniferous|Carboniferous|||||||07-FEB-11
23746|Macauley Creek Granite|42407|6|Mentioned|p44|||Reserved 1988.||||||
23746|Macauley Creek Granite|42689|5|Briefly described|map legend|Carboniferous||||||||
23746|Macauley Creek Granite|42690|5|Briefly described|map legend|Carboniferous||||||||
23746|Macauley Creek Granite|42692|5|Briefly described|map legend|Carboniferous||||||||
23746|Macauley Creek Granite|43095|2|Defined|p44|Late Carboniferous|Early Carboniferous|K-Ar age of 306 Ma but sample affected by argon loss.||||||02-JUL-15
23746|Macauley Creek Granite|43589|2|Defined|p21|Early Carboniferous|Early Carboniferous|Intrudes Running River and Argentine Metamorphics; also inferred to to be intruded by Spinifex Creek Granite. This granite and Spinifex Creek Granite were previously mapped as Oweenee Granite by Wyatt and others (1970).||||||16-MAR-10
23746|Macauley Creek Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink to grey, medium- to coarse-grained, equigranular biotite granite.|
23746|Macauley Creek Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink to grey, medium- to coarse-grained, equigranular biotite granite.|
23746|Macauley Creek Granite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Is intruded by Spinifex Creek Granite.|Pink to grey, medium to coarse-grained, equigranular biotite granite.|
23746|Macauley Creek Granite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Is intruded by Spinifex Creek Granite.|Pink to grey, medium to coarse-grained, equigranular biotite granite.|
23746|Macauley Creek Granite|69592|5|Briefly described|p275|Mississippian|Mississippian|NE margin of the Sybil Graben.||||Is faulted against the Sybil Group.||
23746|Macauley Creek Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
79721|Machattie beds|70673|5|Briefly described|p2, p10, p35-40|||Carr et al. (2014).|1074 +/- 23 Ma (Maximum depositional age).||||Includes quartzite.|
79721|Machattie beds|70749|5|Briefly described|p43-45, p48-53, p55|Cambrian|Neoproterozoic|New, informal name. Undercover Thomson Orogen. Marine deposits: deep-water to near storm-wave base. Only mildly deformed. Abundant 1300-900 Ma (detrital) zircons, derived from the Musgrave Province. SHRIMP U-Pb zircon age determinations from GSQ Machattie 1. Lu-Hf and O isotopic results discussed. Also appears as Machattie Beds on p50-53.|626 +/- 16 Ma (maximum depositional age).||||Moderately dipping, interbedded fine- to medium-grained quartz-feldspar-lithic sandstone and pebbly sandstone, planar laminated dark grey shale and minor thin siltstone interbeds.|
79721|Machattie beds|71031|6|Mentioned|p7|||Thomson Orogen.||||||
79721|Machattie beds|71966|5|Briefly described|p989-990|Cambrian|Neoproterozoic|Geological province: Thomson Orogen. Occurs near the western margin of the Thomson Orogen, and can be considered as late Neoproterozoic to early Cambrian sediments undercover (Carr et al., 2014). Intersected in GSQ Machattie 1 and Goleburra 1; maximum depositional ages of 626+\-16 Ma and 1074+\-520 Ma respectively.||||Overlain by Thomson beds.||
79721|Machattie beds|73177|6|Mentioned|p1113|||Purdy et al. (2016).||||||
33151|Macksford Volcanics|60480|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Andesite and basalt lava, breccia and volcanic arenite.||||||
33151|Macksford Volcanics|61035|6|Mentioned|p52 |Carboniferous|Devonian |Of the Connors Volcanics. Geological Province: Connors Subprovince.||||||07-FEB-11
33151|Macksford Volcanics|65388|4|Described|p110-111, p86, 85, 86, 124, 128, 359.|Middle Carboniferous||Of Connors Volcanic Group, Connors Arch. Volcanic rocks underling the Coppermine Andesite and appear to overlie the Leura and Clive Creek Volcanics. Intruded by South Creek Quartz Diorite. Lithologically identical to Mount Benmore Volcanics. Age equivalent to Ametdale Volcanics? Basalt or andesite flows and volcaniclastic rocks. SHRIMP Age: 315+/- 4 Ma, but based on only 3 grains.||||||
33151|Macksford Volcanics|68679|4|Described|p355, p357|||Connors Subprovince. Restricted to a narrow belt ~0.5km wide, extending ~3.5km NNW from Mount Mackenzie. May be older than the Tartrus Rhyolite [??-is said to overlie Tartrus Volcanics on p357]. The rocks are affected by the Mount Mackenzie alteration system. See also reference to Macksford Andesite (p353). This age is a minimum, from the intrusion.|304 +/- 2 Ma : Burch (1999).|Connors Volcanic Group.||Overlies the Leura Volcanics and Tartrus Rhyolite (but see COMMENTS). Is intruded by the South Creek Diorite.|Basalt or andesite flows and poorly bedded volcaniclastic rocks. Epidote alteration is common.|
33151|Macksford Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Andesite.|
36316|Madjack Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36316|Madjack Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink, medium- to coarse-grained biotite monzogranite; minor microgranite.|
27472|Magazine Shale|23031|6|Mentioned|27|||Geol province Leichardt River Subprovince. Parent Mount Isa Group||||||
27472|Magazine Shale|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group.||||||07-NOV-08
27472|Magazine Shale|23399|4|Described|p487|||Of Mount Isa Group.||||||01-OCT-08
27472|Magazine Shale|23408|5|Briefly described|p511, p523, p527|||Of Mount Isa Group. Sediments are fine-grained, rhythmically laminated siltstone and shale.||||||15-JUN-09
27472|Magazine Shale|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
27472|Magazine Shale|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: Mount Isa Group||||||07-NOV-08
27472|Magazine Shale|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Mount Isa Group. Overlies Spear Siltstone. Geological Province: Leichardt River Fault Trough.||||||
27472|Magazine Shale|30535|6|Mentioned|p403|||Refers Bennett(1965). See also p405||||||16-MAR-18
27472|Magazine Shale|31207|6|Mentioned|Table 1|||||||||
27472|Magazine Shale|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27472|Magazine Shale|32041|4|Described|p356|||||||||
27472|Magazine Shale|32042|5|Briefly described|p44|||||||||
27472|Magazine Shale|32376|6|Mentioned|Table 3|||||||||
27472|Magazine Shale|32660|5|Briefly described|Table 5|||||||||
27472|Magazine Shale|32959|6|Mentioned|Fig.21|||||||||
27472|Magazine Shale|33900|5|Briefly described|p14|||||||||
27472|Magazine Shale|34499|6|Mentioned|Table 1|||||||||
27472|Magazine Shale|34754|6|Mentioned|p42|||||||||
27472|Magazine Shale|35074|6|Mentioned|Fig.2|||||||||
27472|Magazine Shale|35116|6|Mentioned|Table.4|||||||||
27472|Magazine Shale|39445|5|Briefly described|Table 2|||||||||
27472|Magazine Shale|39561|6|Mentioned|Fig.8|||||||||
27472|Magazine Shale|41248|6|Mentioned|Fig.7|||||||||
27472|Magazine Shale|41298|6|Mentioned|Map legend|Carpentarian||||||||
27472|Magazine Shale|42350|6|Mentioned|Fig.1 P543|||||||||
27472|Magazine Shale|42782|6|Mentioned|p458|||of Mount Isa Group||||||
27472|Magazine Shale|43760|6|Mentioned|p441|||||||||
27472|Magazine Shale|44517|2|Defined|p235-236,243,map||Paleoproterozoic|Unit of Mount Isa Group.||||||07-NOV-08
27472|Magazine Shale|44843|14|Not recorded|p175|||||||||
27472|Magazine Shale|45072|6|Mentioned|p8|||Mount Isa Group||||||
27472|Magazine Shale|45136|6|Mentioned|p49|||||||||
27472|Magazine Shale|45166|5|Briefly described|p28|||||||||
27472|Magazine Shale|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
27472|Magazine Shale|50624|5|Briefly described|p237 Fig.4||Statherian|Parent: Mount Isa Group.||||||
27472|Magazine Shale|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Underlain by Kennedy Siltstone. Geological Province: Western Fold Belt.||||||03-JUN-09
27472|Magazine Shale|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Isa Superbasin, Western Fold Belt, Mount Isa Inlier. ||||||
27472|Magazine Shale|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Mount Isa.||Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
27472|Magazine Shale|62535|5|Briefly described|p672|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified.||Mount Isa Group.||||
27472|Magazine Shale|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
27472|Magazine Shale|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Magazine.||Of the Loretta supersequence||||
27472|Magazine Shale|63866|5|Briefly described|p59|||Isa Superbasin.||Gun Supersequence||Equivalent to the overlying Loretta Supersequence.||
27472|Magazine Shale|64250|6|Mentioned|p11 fig 3|||||Unit in Mount Isa Group.||||
27472|Magazine Shale|65228|6|Mentioned|p26, Fig.04.|||Part of Loretta Supersequence at Mount Isa.||||||
27472|Magazine Shale|65396|5|Briefly described|p82, p175, p241|||Isa Superbasin. Cover Sequence 3. Leichhardt River Fault Trough.||Mount Isa Group||Overlies Spear-Kennedy Siltstone.||04-APR-17
27472|Magazine Shale|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
27472|Magazine Shale|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Isa Superbasin.|~1660-1650 Ma.|Mount Isa Group.|||Thin-bedded calcareous sericitic shale with minor pyrite.|
27472|Magazine Shale|68542|6|Mentioned|p6|||||||Overlies Kennedy Siltstone||
27472|Magazine Shale|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Kennedy Siltstone.||
27472|Magazine Shale|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|The lithology is not specified; this unit appears only as Magazine Kennedy Siltstone [?Magazine and Kennedy Siltstones]. Sedimentary depositional age. Of the Loretta Supersequence.|1647 +/- 4 Ma|||||01-DEC-17
27472|Magazine Shale|69591|5|Briefly described|p45, p55|||Leichhardt River Domain. Part of Loretta Supersequence. Below storm base deposits.||Mount Isa Group.|||Thin-bedded calcareous sericitic shale with minor pyrite.|
27472|Magazine Shale|70282|6|Mentioned|p544 fig 1|||||||Overlies Kennedy-Spear Siltstone,||
27472|Magazine Shale|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Overlies Spear-Kennedy Siltstone.||
27472|Magazine Shale|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Overlies Spear-Kennedy Siltstone.||
27472|Magazine Shale|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Isa Superbasin.||Mt Isa Group||Underlain by Spear-Kennedy Siltstone.||
27472|Magazine Shale|73525|5|Briefly described|p4-5 Fig.2|||Leichhardt River Domain.|||||Carbonaceous shale (-silt) carbonates.|
27185|Magna Lynn Metabasalt|22498|6|Mentioned|Fig1 P234|||||||||
27185|Magna Lynn Metabasalt|22623|6|Mentioned|p225,6|||||||||
27185|Magna Lynn Metabasalt|23054|6|Mentioned|p9|||||||||
27185|Magna Lynn Metabasalt|23071|5|Briefly described|p760|||||||||
27185|Magna Lynn Metabasalt|23079|6|Mentioned|p701|||||||||
27185|Magna Lynn Metabasalt|23205|6|Mentioned|p43|||of Mt Isa Inlier.||||||
27185|Magna Lynn Metabasalt|23518|4|Described|p10|Proterozoic|Proterozoic|Of Tewinga Group.  Geological Province: Kalkadoon-Ewen Province.||||||
27185|Magna Lynn Metabasalt|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Tewinga Group.  Overlies the Leichhardt Metamorphics; underlies the Argylla Formation.||||||25-AUG-04
27185|Magna Lynn Metabasalt|30536|2|Defined|p98|Carpentarian|Carpentarian|||||||
27185|Magna Lynn Metabasalt|32660|5|Briefly described|Table 5|||||||||
27185|Magna Lynn Metabasalt|32959|6|Mentioned|Fig.21|||||||||
27185|Magna Lynn Metabasalt|33900|4|Described|p9|||Mention p7.||||||18-JAN-07
27185|Magna Lynn Metabasalt|35074|4|Described|p212|||Mentioned on p206.||||||18-JAN-07
27185|Magna Lynn Metabasalt|35286|6|Mentioned|p143|||||||||
27185|Magna Lynn Metabasalt|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27185|Magna Lynn Metabasalt|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27185|Magna Lynn Metabasalt|37462|4|Described|Table4.VII|||||||||
27185|Magna Lynn Metabasalt|37568|6|Mentioned|p81|||||||||
27185|Magna Lynn Metabasalt|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27185|Magna Lynn Metabasalt|37862|6|Mentioned|p581|||||||||
27185|Magna Lynn Metabasalt|38234|4|Described|p101|||||||||
27185|Magna Lynn Metabasalt|38238|6|Mentioned|p135|||||||||
27185|Magna Lynn Metabasalt|38276|6|Mentioned|Fig.1|||||||||
27185|Magna Lynn Metabasalt|38350|4|Described|p6|||||||||
27185|Magna Lynn Metabasalt|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27185|Magna Lynn Metabasalt|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27185|Magna Lynn Metabasalt|38834|6|Mentioned|p162|||||||||
27185|Magna Lynn Metabasalt|38900|6|Mentioned|Fig.2|||||||||
27185|Magna Lynn Metabasalt|39202|6|Mentioned|Fig.2|||||||||
27185|Magna Lynn Metabasalt|39445|5|Briefly described|Table 2|||See also p35 and p39.||||||18-JAN-07
27185|Magna Lynn Metabasalt|39496|6|Mentioned|p5|||||||||
27185|Magna Lynn Metabasalt|39622|6|Mentioned|p19|||||||||
27185|Magna Lynn Metabasalt|39799|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle ProterozoicE - M||||||07-NOV-08
27185|Magna Lynn Metabasalt|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27185|Magna Lynn Metabasalt|39924|6|Mentioned|p348|||||||||
27185|Magna Lynn Metabasalt|39937|6|Mentioned|Fig.1|||||||||
27185|Magna Lynn Metabasalt|40623|5|Briefly described|p95|||||||||
27185|Magna Lynn Metabasalt|40648|3|Fully described|p6|||||||||
27185|Magna Lynn Metabasalt|40840|6|Mentioned|Map legend|||||||||
27185|Magna Lynn Metabasalt|40984|6|Mentioned|p389|||||||||
27185|Magna Lynn Metabasalt|41381|6|Mentioned|p323|||||||||
27185|Magna Lynn Metabasalt|41465|5|Briefly described|p11|||||||||
27185|Magna Lynn Metabasalt|41744|6|Mentioned|p406|||||||||
27185|Magna Lynn Metabasalt|41761|6|Mentioned|Fig.1|||||||||
27185|Magna Lynn Metabasalt|41791|6|Mentioned|p269|||||||||
27185|Magna Lynn Metabasalt|41978|6|Mentioned|p495|||||||||
27185|Magna Lynn Metabasalt|42365|5|Briefly described|Fig.3 P258|||||||||
27185|Magna Lynn Metabasalt|42565|4|Described|Table 1 P6, P2|||||||||
27185|Magna Lynn Metabasalt|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Mafic volcanics, minor sandstone.||||||09-FEB-09
27185|Magna Lynn Metabasalt|42818|5|Briefly described|Fig.2 P205|||||||||
27185|Magna Lynn Metabasalt|42858|5|Briefly described|Fig.1 P671|||||||||
27185|Magna Lynn Metabasalt|42859|5|Briefly described|p675|||||||||
27185|Magna Lynn Metabasalt|43052|5|Briefly described|p100|||||||||
27185|Magna Lynn Metabasalt|43616|6|Mentioned|p3|||||||||
27185|Magna Lynn Metabasalt|43643|5|Briefly described|p612|||||||||
27185|Magna Lynn Metabasalt|45136|3|Fully described|p16|||||||||
27185|Magna Lynn Metabasalt|45161|4|Described|p19|||See also Table 5||||||
27185|Magna Lynn Metabasalt|45166|6|Mentioned|p7|||||||||
27185|Magna Lynn Metabasalt|46801|6|Mentioned|Fig. 14|||||||||
27185|Magna Lynn Metabasalt|46859|6|Mentioned|p311|||||||||
27185|Magna Lynn Metabasalt|46960|6|Mentioned|Fig.3|||||||||
27185|Magna Lynn Metabasalt|46962|4|Described|Table 1|||See also Fig.3.||||||
27185|Magna Lynn Metabasalt|46995|5|Briefly described|p267|||||||||
27185|Magna Lynn Metabasalt|46996|6|Mentioned|p273|||||||||
27185|Magna Lynn Metabasalt|49009|6|Mentioned|p5|||||||||
27185|Magna Lynn Metabasalt|49041|6|Mentioned|p3|||||||||
27185|Magna Lynn Metabasalt|50100|5|Briefly described|p14 Fig. 5, p17, p78|Proterozoic|Proterozoic|Basaltic lava flows, some intercalated clastic sedim. rocks and minor felsic volcs.  Unconformably overlies Leichhardt Volcs and Kalkadoon Granodiorite; overlain by Stanbroke Sst; conformably overlain by Argylla Fm. Geol.Prov: Kalk.-Ewen Prov/Wonga Subpr||||||20-JAN-05
27185|Magna Lynn Metabasalt|50125|6|Mentioned|p100|||Geological Province: Mount Isa Inlier||||||
27185|Magna Lynn Metabasalt|50332|4|Described|p17|Proterozoic|Proterozoic|Unconformably underlain by Leichhardt Volcanics + Kalkadoon Granodiorite. Geol Prov: Kalkadoon-Ewen Province + Wonga Subprovince. Unit consits of a series of basaltic lava flows + intercalated clastic sedimentary rocks + minor felsic volcanics.||||||07-FEB-11
27185|Magna Lynn Metabasalt|50536|5|Briefly described|p4.1, 5.3|||Geological Province: Mount Isa Inlier. Intruded by the Wonga Suite.||||||
27185|Magna Lynn Metabasalt|50605|6|Mentioned|p11.3|||||||||
27185|Magna Lynn Metabasalt|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metabasalt, meta-arenite, mafic schist, conglomerate. Of the Tewinga Group.||||||26-AUG-04
27185|Magna Lynn Metabasalt|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block and Eastern Fold Belt.||||||03-JUN-09
27185|Magna Lynn Metabasalt|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1800Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
27185|Magna Lynn Metabasalt|61922|5|Briefly described|p8, p17 Fig. 9|||Part of a bimodal suite unconformably overlying the Leichhardt Volcanics. Interfingered with the Argylla Formation. Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
27185|Magna Lynn Metabasalt|61924|5|Briefly described|p44|||||||||
27185|Magna Lynn Metabasalt|64248|6|Mentioned|p38 Fig.5|||||||||
27185|Magna Lynn Metabasalt|64250|5|Briefly described|Figs.3,5,8, 10; p19, p21,|||At base of Leichhardt Superbasin, Kalkadoon-Leichhardt Belt. Mis-spelt as Magna Lyn in Fig.10.|~1780 Ma|||Extruded at same time as Eastern Creek Volcanics.|Mafic lavas.|
27185|Magna Lynn Metabasalt|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
27185|Magna Lynn Metabasalt|65376|5|Briefly described|p231.|||Geochemically similar to Myola Volcanics and felsic units of Tidnamurkuna Volcanics.|c.1790 Ma.|||||
27185|Magna Lynn Metabasalt|65387|5|Briefly described|p60, p77|||The Magna Lynn Metabasalt appears to be metasomatically intruded by the (younger) Leichhardt Volcanics porphyry.||||Disconformably overlies and interdigitates with Leichhardt Volcanics. Occurs as enclaves within Argylla suite.||
27185|Magna Lynn Metabasalt|65396|5|Briefly described|p7, p16, p82, p84, p175, p183, p187,p190|||See also p192-193, p241, p439. Leichhardt Superbasin: Eastern Succession. Cover Sequence 2. Kalkadoon-Leichhardt Belt.|c.1780 Ma.|||Overlain by Argylla Formation.|Metabasalt, minor mafic volcanics, felsic volcanics and sandstone/quartzite.|
27185|Magna Lynn Metabasalt|65505|6|Mentioned|966, 979, Fig 1,3|Proterozoic|Proterozoic|Co-magmatic with the Argylla Formation; together represent a wide-spread, voluminous magmatic event between c.1780 and 1775 Ma in the Mary Kathleen region.||||||
27185|Magna Lynn Metabasalt|67323|5|Briefly described|GIS attrib tbl, p14, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Erupted during extension of Leichhardt Superbasin. Appears as Magna Lynn Basalt on p31.|~1780-1760 Ma.||||Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz +/- feldspar porphyry.|
27185|Magna Lynn Metabasalt|67539|6|Mentioned|p10, p11|||||||Underlain by the Leichhardt Volcanics.|Local quartzite lenses.|
27185|Magna Lynn Metabasalt|68542|6|Mentioned|p12|||||||||
27185|Magna Lynn Metabasalt|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with Argylla Formation under the symbol, -Pva.||||||
27185|Magna Lynn Metabasalt|68575|6|Mentioned|p75|||||||||
27185|Magna Lynn Metabasalt|68576|6|Mentioned|Q_2: p12|||Contemporaneous with Argylla Formation.||||||
27185|Magna Lynn Metabasalt|69056|6|Mentioned|p2, Reference images sheet|||Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Argylla Formation.||||||
27185|Magna Lynn Metabasalt|69222|6|Mentioned|p222 Fig.2, p223|Statherian|Statherian|Kalkadoon-Leichhardt Fold Belt. Extruded during the Leichhardt Rift Event.||||Overlain by Argylla Formation||09-FEB-18
27185|Magna Lynn Metabasalt|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Is overlain by Argylla Formation.||25-JAN-19
27185|Magna Lynn Metabasalt|69591|5|Briefly described|p29-30, p33-34, p58, p105|Paleoproterozoic|Paleoproterozoic|Kalkadoon-Leichhardt Domain, Leichhardt Superbasin, Mount Isa Province. Part of Guide and ?Myally Supersequences.|~1780 Ma.|||Is overlain by Argylla Formation.|Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz +/- feldspar porphyry. Highly magnetic.|
27185|Magna Lynn Metabasalt|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The two facies associations are mapped separately.|||||Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz-feldspar porphyry. Pebbly metasandstone and quartzite, calcareous quartzite, para-amphibolite and mica schist.|
27185|Magna Lynn Metabasalt|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The two facies associations are mapped separately.|||||Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz-feldspar porphyry. Pebbly metasandstone and quartzite, calcareous quartzite, para-amphibolite and mica schist.|
27185|Magna Lynn Metabasalt|71799|5|Briefly described|p150 fig 2, p151 fig 3, p152|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block. Provisionally correlated with the Cromwell Metabasalt Member.|ca. 1800 Ma||||Thick metabasalt flows.|
27185|Magna Lynn Metabasalt|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||||Shown as overlying Kalkadoon Granite and underlies and is partially laterally equivalent to Argylla Formation.||
27185|Magna Lynn Metabasalt|72596|6|Mentioned|p49|||||||Intruded by Bowlers Hole Granite.|Mainly metavolcanic rocks.|
27185|Magna Lynn Metabasalt|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Mary Kathleen Domain and Kalkadoon-Leichhardt Domain. Maximum age poorly constrained. Includes marker bed of epidotic quartzite, meta-arenite. Two additional informal sub-units shown.||||Shown as older than Argylla Formation.|Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz-feldspar porphyry. Also biotite schist, minor felsic volcanics, pods of foliated gneissic granite and augen gneiss, pebbly metasandstone and calcareous quartzite.|
27185|Magna Lynn Metabasalt|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of both the Mary Kathleen Domain and Kalkadoon-Leichhardt Domain. Maximum age poorly constrained. Includes marker bed of epidotic quartzite, meta-arenite. Two additional informal sub-units shown.||||Shown as older than Argylla Formation.|Metabasalt, amphibolite; minor quartzite, meta-arenite, mafic schist and quartz-feldspar porphyry. Also biotite schist, minor felsic volcanics, pods of foliated gneissic granite and augen gneiss, pebbly metasandstone and calcareous quartzite.|
27185|Magna Lynn Metabasalt|72889|6|Mentioned|p6 Fig.i.|||||||||
27185|Magna Lynn Metabasalt|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Kalkadoon-Leichhardt Belt of the Mount Isa Province. U-Pb zircon igneous crystallisation age (Ma) shown. See also Magna Lynn Volcanics p12.||||Shown as underlying Argylla Formation.||
27185|Magna Lynn Metabasalt|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||||Overlain by and partly equivalent to Argylla Formation.||
27185|Magna Lynn Metabasalt|73137|6|Mentioned|p1, p6, p90, p95, p99|Paleoproterozoic|Paleoproterozoic|Interpreted to pre-date Bushy Park Gneiss and Birds Well Granite [proper].||||||
27185|Magna Lynn Metabasalt|73413|6|Mentioned|p3, p6|Statherian|Statherian|Mount Isa Inlier, Kalkadoon-Leichhardt Belt. Constitutes the stratigraphic base of Cover Sequence 2 (of Foster and Austin, 2008). [Age written as ca. 1790 Ma and 1800-1775 Ma].|ca. 1790 Ma|||Overlain by Argylla Formation.||
27185|Magna Lynn Metabasalt|73525|6|Mentioned|p4, p17, p19 Fig.13, p20|||Kalkadoon-Leichhardt Domain.|||||Mafic succession. Includes siliciclastics.|
27185|Magna Lynn Metabasalt|73529|5|Briefly described|p2 Fig.1, p4, p6 Fig.3, p8, p14|||Mary Kathleen Domain. Base of Mary Kathleen Group.||||Underlies Argylla Formation|Volcanic unit.|09-MAR-23
27185|Magna Lynn Metabasalt|73553|5|Briefly described|p1, p6, p8, p14, p18-24, p42,|Statherian|Statherian|Oldest unit of Mary Kathleen Domain. Exposed in an up to 3km wide and >200km long belt along the western margin of the domain. Unconformably overlies Kalkadoon-Leichhardt Domain. Described by Derrick et al., (1977a), Wilson et al., (1977), Bultitude et al., (1982a), and Wilson (1982). Previously included in unnamed unit 'db' by Carter (1959) and Carter and Opik (1963). Included in the Tewinga Group of Derrick et al., (1997a). Maximum thickness of ~1300 m. Undated. Subaerial to shallow marine depositional environment. Minor copper mineralisation is common throughout. Interpreted to be intruded by Scheelite Granite. Rocks mapped as Magna Lynn Metabasalt are interlayered with Bushy Park Gneiss. See also p63, p73, p99, p122-125, p187-189, p230-231, p246.|1800-1775 Ma|||Unconformably overlies Leichhardt Volcanics, conformably underlies Argylla Formation with local interfingering, intruded by Bowlers Hole Granite, Mairindi Creek Granite, Birds Well Granite|Dominantly dark grey to greenish black, fine-grained, epidotic, amygdaloidal metabasalt. Contains lenses of quartzite, sandstone, siltstone, breccia, tuff, felsic volcanics, and thick intercalations of sedimentary rocks.|03-FEB-23
41804|Magog Gabbro|60481|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Coarse to very coarse grained hornblende gabbro with minor hornblende monzonite.||||||
41804|Magog Gabbro|61035|5|Briefly described|p17 Tb. 2|Triassic|Permian|Intrudes Marlborough Metamorphics. Consists of very coarse-grained hornblende gabbro with minor hornblende monzonite.||||||07-FEB-11
41804|Magog Gabbro|65388|4|Described|p431, p70 Fig. 28, p153, 432|Late Permian|Late Permian|Intrudes Marlborough Metamorphics. May be intruded by Og Syenite [?see Og Syenite, same page]. 40Ar/39Ar step-heating dating ~255+/-2Ma, with resetting at 242+/-3Ma. Coarse to very coarse-grained hornblende gabbro with minor hornblende monzonite.||||||08-SEP-14
41804|Magog Gabbro|68679|5|Briefly described|p308-309, p424, p426|Permian|Permian|Marlborough Province. ~12 km2 in the Magog Range, forming Mount Magog and Mount Gog. Harbort (2001) also identified a thermal pulse at 242 +/- 3 Ma, an identical age to the determination of Magog Gabbro by Webb and McDougall (1968).|255 +/- 2 Ma (Ar-Ar: Harbort, 2001).|||Intrudes Marlborough Metamorphics. May be intruded by Og Syenite.|Hornblende gabbro with minor hornblende monzonite.|
23748|Magpie Creek Limestone Member|23032|5|Briefly described|p22|Pridoli|Ludlow|||||||
23748|Magpie Creek Limestone Member|23424|5|Briefly described|Table 8.1||Llandovery|Of Quinton Formation/Graveyard Creek Group, Graveyard Creek Subprovince. Maximum thickness 500 m.||||||
23748|Magpie Creek Limestone Member|23431|5|Briefly described|p541|||Of Quinton Formation.||||||
23748|Magpie Creek Limestone Member|24029|5|Briefly described|p112 Fig.1|||Of Graveyard Creek Group.||||||
23748|Magpie Creek Limestone Member|41260|4|Described|p41|||See also p145. Mention p115.||||||10-APR-08
23748|Magpie Creek Limestone Member|41679|6|Mentioned|Fig.2|||||||||
23748|Magpie Creek Limestone Member|41719|2|Defined|p217|Late Silurian||||||||
23748|Magpie Creek Limestone Member|41739|6|Mentioned|Fig.2|||||||||
23748|Magpie Creek Limestone Member|41740|6|Mentioned|p222|||||||||
23748|Magpie Creek Limestone Member|42054|6|Mentioned|p273|||||||||
23748|Magpie Creek Limestone Member|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
23748|Magpie Creek Limestone Member|42933|3|Fully described|p58|Late Silurian||of Quinton Formation||||||
23748|Magpie Creek Limestone Member|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Quinton Formation.||||||
23748|Magpie Creek Limestone Member|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Quinton Formation.|||Limestone (calcilutite to pelloidal calcarenite) and minor mudstone; local breccia or calcirudite.|
23748|Magpie Creek Limestone Member|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Quinton Formation.|||Limestone (calcilutite to pelloidal calcarenite) and minor mudstone; local breccia or calcirudite.|
23748|Magpie Creek Limestone Member|69030|5|Briefly described|p6|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province). The rank of Member is omitted in the diagram.||Quinton Formation.||||12-SEP-16
23748|Magpie Creek Limestone Member|69592|5|Briefly described|p263|Lochkovian|Ludlow|Previously a unit in the Quinton Formation. It and the rest of the upper part of that Formation, with part of the Jack Formation, were assigned by Mawson and Talent (2000) to their Ralph Flint Formation. Appears on the same page as Magpie Creek Member.||||||
79158|Mailmans Gap Granodiorite|69952|5|Briefly described|p2 Tb.i, p5, p72-78|Middle Permian|Middle Permian|New England Orogen. 90km N of Rockhampton, and ~3.5 km E of the main Pyri Pyri Batholith. Generally deeply weathered; forms recessive country bounded by hills of Shoalwater Formation. This mid-Permian SHRIMP U-Pb zircon magmatic crystallisation age resolves uncertainty about possible Cretaceous [or Triassic] age. Suggests a similar age for Pyri Pyri Granite. May be comagmatic with Double Mountain Volcanics (whose crystallisation age of 270.6 +4.6/-2.2 Ma is indistinguishable).|269.3 +/- 1.9 Ma (Cross et al., 2015).||||Pale grey, fine- to medium-grained, moderately porphyritic granodiorite with sparse mafic inclusions; monzogranite. Oxidised I-type.|28-AUG-15
79158|Mailmans Gap Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|269+/-1.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
79158|Mailmans Gap Granodiorite|73197|6|Mentioned|p475 Fig.6, 476|Guadalupian|Guadalupian|New England Orogen, northern.|269 Ma U-Pb|||||
67885|Main Pipe Breccia|24424|5|Briefly described|p525|Early Permian|Early Permian|Matrix supported breccia with basement clasts. Of Mount Leyshon Intrusive Complex. Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
67885|Main Pipe Breccia|62077|5|Briefly described|p34-36, p37 Fig.2|||Represents the earliest stage of hydrothermal activity in the Mount Leyshon Intrusive Complex. Has a strong, negative magnetic anomaly due to biotite (+/- magnetite) alteration.||Unit in Mount Leyshon Intrusive Complex.||Is intruded by Mount Leyshon Breccia.|Clast- to matrix-supported breccia composed of variably rounded clasts of basement lithologies.|
24369|Mairindi Creek Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Argylla Suite. Intrusive rocks. Age: 1780Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24369|Mairindi Creek Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24369|Mairindi Creek Granite|37862|4|Described|p585|||||||||
24369|Mairindi Creek Granite|38350|4|Described|p17|||||||||
24369|Mairindi Creek Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24369|Mairindi Creek Granite|38658|6|Mentioned|p152|||||||||
24369|Mairindi Creek Granite|39445|5|Briefly described|Table 2|||||||||
24369|Mairindi Creek Granite|40840|6|Mentioned|Map legend|||||||||
24369|Mairindi Creek Granite|41978|6|Mentioned|p501|||||||||
24369|Mairindi Creek Granite|45161|5|Briefly described|p31|||||||||
24369|Mairindi Creek Granite|45166|5|Briefly described|p34|||||||||
24369|Mairindi Creek Granite|49009|2|Defined|p23|Proterozoic|Proterozoic|Previously mapped as Kalkadoon Granite (Carter & Opik,1963).||||||
24369|Mairindi Creek Granite|49041|5|Briefly described|Table 2|||||||||
24369|Mairindi Creek Granite|50100|5|Briefly described|p13 Fig. 4|Statherian|Statherian|Intrudes the Argylla Formation.||||||
24369|Mairindi Creek Granite|50536|5|Briefly described|p1.4, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Argylla Suite.||||||07-NOV-08
24369|Mairindi Creek Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite-hornblende granite.||||||
24369|Mairindi Creek Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Kalkadoon Igneous Event.|1777 +/- 7 Ma.|Kalkadoon Supersuite||Intrudes Argylla Formation.|Foliated hornblende-biotite granite.|
24369|Mairindi Creek Granite|67497|6|Mentioned|p909|Statherian|Statherian||~1780 Ma|Of the Argylla Suite|||A-type granite|
24369|Mairindi Creek Granite|69591|5|Briefly described|p60|||Wonga Batholith.|||||Foliated hornblende-biotite granite.|
24369|Mairindi Creek Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Foliated hornblende-biotite granite.|
24369|Mairindi Creek Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Foliated hornblende-biotite granite.|
24369|Mairindi Creek Granite|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Statherian|Statherian|Kalkadoon-Leichhardt Domain.|ca. 1775 Ma, 1777+/-7 Ma crystallisation age||||Felsic intrusive.|
24369|Mairindi Creek Granite|73553|4|Described|p2-3, p8, p14, p27, p43-45, p53, p56,|Statherian|Statherian|Mary Kathleen Domain. Argylla Igneous Province intrusion. Small, roughly rectangular pluton northwest of Duchess. Felsic granite, with evidence of potash metasomatism. Intruded by numerous amphibolitic metadoleritic dykes, and thin aplite and quartz veins. Subalkaline, slightly peraluminous, A-type. Included in Argylla Suite by Budd et al., (2001). See also p58-59, p61-65, p117, p157-158, p247, p249, p266.|~1770 Ma LA-ICP-MS zircon|Argylla Suite||Intrudes Argylla Formation, Magna Lynn Metabasalt|Pink, partly recrystallised, medium-grained, uneven-grained to slightly porphyritic biotite granite, well-developed foliation.|03-FEB-23
24370|Makowata Oil Shale Member|40247|6|Mentioned|p212|||Mention Fig.4||||||
24370|Makowata Oil Shale Member|40954|6|Mentioned|p133|||||||||
24370|Makowata Oil Shale Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably overlain by the Sonoma Member. Conformably underlain by the Korenan Oil Shale Member.|Brownish black, thinly laminated oil shale; minor interbedded claystone; some massive olive-grey claystone beds.|
24370|Makowata Oil Shale Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. 18.4 - 73.5m thick, averaging 36.3m.||Lowmead Formation.||Overlies Korenan Oil Shale Member. Is overlain by Sonoma Member.|Carbonaceous oil shale, minor interbedded claystone.|
24371|Malacura Sandstone|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Langlovale Group. Sandstone, siltstone, carbonaceous mudstone.||||||13-MAY-15
24371|Malacura Sandstone|23291|4|Described|p26, p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Langlovale Group. Geological Province: Georgetown Region.||||||13-MAY-15
24371|Malacura Sandstone|35921|2|Defined|p41|Mesoproterozoic|Mesoproterozoic|||||||
24371|Malacura Sandstone|36153|6|Mentioned|Fig.10|||||||||
24371|Malacura Sandstone|36216|6|Mentioned|p208|||||||||
24371|Malacura Sandstone|36780|6|Mentioned|Fig.10|||||||||
24371|Malacura Sandstone|36937|6|Mentioned|p229|||||||||
24371|Malacura Sandstone|38716|6|Mentioned|p193|||||||||
24371|Malacura Sandstone|39445|5|Briefly described|Table 2|||See also P37 & P45||||||
24371|Malacura Sandstone|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24371|Malacura Sandstone|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24371|Malacura Sandstone|40860|6|Mentioned|Fig.2|||||||||
24371|Malacura Sandstone|41975|4|Described|p437|||||||||
24371|Malacura Sandstone|43664|4|Described|p54|||||||||
24371|Malacura Sandstone|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Langlovale Group.||||||
24371|Malacura Sandstone|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Part of the Langlovale Group.||||||05-JUL-04
24371|Malacura Sandstone|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Langlovale Group. Lithic quartz and quartz sandstone, commonly feldspathic and and micaceous.||||||13-MAY-15
24371|Malacura Sandstone|63866|5|Briefly described|p77|||Interpreted to have been deposited in a fluvial environment.||Langlovale Group||||
24371|Malacura Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||||Is intruded by Esmeralda and Lighthouse Supersuites.||
24371|Malacura Sandstone|67341|5|Briefly described|vi, p25-28|||Croydon Subprovince, Etheridge Province. Maximum depositional age.|1625 +/- 5 Ma (SHRIMP U-Pb zircon).|Langlovale Group.||Overlies Yarman Formation.|Includes poorly sorted, gritty, coarse- to fine-grained sandstone and reworked, thinly-bedded siltstone.|
24371|Malacura Sandstone|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.||Is overlain conformably by Yarman Formation.|Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.||Is overlain conformably by Yarman Formation.|Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.||Unit in Langlovale Group.|||Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.|||Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.|||Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Savannah Province. Shown as older than D2 (~ 1550-1560 Ma) and younger than D1 (> 1560 Ma , < 1590 Ma).|~ 1590?-1550 Ma|Of the Langlovale Group.|||Feldspathic to sublithic, locally micaceous sandstone; minor locally carbonaceous mudstone and siltstone.|
24371|Malacura Sandstone|69591|5|Briefly described|p70|||See also references to Malacura Formation (p61, p68, p69 Fig.2.65, p70).||Basal Langlovale Group.||Is overlain gradationally by Yarman Formation.|Predominantly immature, poorly sorted, micaceous, feldspathic, possibly fluviatile sandstone; increasing mudstone and sedimentary structures towards the top.|
24371|Malacura Sandstone|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1625+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
27646|Malairo Rhyolite Member|23422|5|Briefly described|p183|Late Carboniferous|Late Carboniferous|Of Hells Gate Rhyolite.||||||
27646|Malairo Rhyolite Member|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|of Hells Gate Rhyolite, Sybil Group.||||||
27646|Malairo Rhyolite Member|23893|5|Briefly described|p18|Carboniferous|Carboniferous|Of Hells Gate Rhyolite.||||||
27646|Malairo Rhyolite Member|42692|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
27646|Malairo Rhyolite Member|43095|1|Redefined|p67|Late Carboniferous||of Hells Gate Rhyolite||||||
27646|Malairo Rhyolite Member|43259|6|Mentioned|Appendix 1,p6.||Carboniferous|Late Carboniferous? in age.||||||
27646|Malairo Rhyolite Member|68350|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Hells Gate Rhyolite.||Is overlain conformably by Engow Member (Marshs Creek Formation).|Flow-banded, commonly spherulitic rhyolitic lava.|
27646|Malairo Rhyolite Member|68351|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Hells Gate Rhyolite.||Is overlain conformably by Engow Member (Marshs Creek Formation).|Flow-banded, commonly spherulitic rhyolitic lava.|
27646|Malairo Rhyolite Member|68731|6|Mentioned|p203|||||Of the Hells Gate Rhyolite.|||Rhyolite flows.|
27646|Malairo Rhyolite Member|69592|5|Briefly described|p275|Permian|Permian|Gunther and Withnall (1992). Sybil Graben.||Hells Gate Rhyolite.|||Rhyolite flows.|
27646|Malairo Rhyolite Member|69593|5|Briefly described|p495|Permian|Late Carboniferous|Younger age may be Late Carboniferous. The parent unit is not identified.|||||Rhyolite lava.|
30704|Malakoff Granite|23519|5|Briefly described|p127|Mesoproterozoic|Mesoproterozoic|Age: 1505+/-5 Ma (U-Pb). See also page 106 Fig 1. Geological Province: Naraku Batholith.||||||
30704|Malakoff Granite|23545|5|Briefly described|p606 Table 1.|||||||||
30704|Malakoff Granite|23967|6|Mentioned|p1331|||||||||
30704|Malakoff Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30704|Malakoff Granite|43490|6|Mentioned|8|||U-Pb Zircon Age: 1505+/-5Ma||||||
30704|Malakoff Granite|50332|5|Briefly described|p22|Mesoproterozoic|Mesoproterozoic|Of the Williams and Naraku Batholiths. Age: 1520-1450Ma. Geological Province: Quamby-Malbon and Cloncurry Subprovinces.||||||18-APR-12
30704|Malakoff Granite|50536|5|Briefly described|p1.5, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite/Supersuite. Age: 1505 +/- 5Ma (SHRIMP).||||||21-JUN-16
30704|Malakoff Granite|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Pluton of the Williams and Naraku Batholiths. Age: 1516-1490 Ma.||||||
30704|Malakoff Granite|63866|5|Briefly described|p62|Calymmian|Calymmian|Tommy Creek Block.|1505-1500 Ma (Page and Sun, 1998)|||||
30704|Malakoff Granite|64250|6|Mentioned|p11 fig 3||||1505 +/- 5 Ma.|||||
30704|Malakoff Granite|65396|6|Mentioned|p7, p53, p56, p82, p84, p175, p241|Calymmian|Calymmian|Kalkadoon-Leichhardt Belt, Mount Isa Inlier. Associated with the Isan Orogeny. Appears as Malakoff granite on p53.|1505 +/- 5 Ma (SHRIMP: Page and Sun, 1998)|||||
30704|Malakoff Granite|66913|5|Briefly described|p171 fig 2, p188|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2. Possibly hydrothermal zircons dated at <1500 Ma.||||||
30704|Malakoff Granite|67323|5|Briefly described|GIS attrib tbl, p17-18|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Intrudes the southern Canobie Domain near Cloncurry. Williams Igneous Event. Main constituent of the Naraku Batholith. Low gravity response. Largely undeformed; post-dates Isan Orogeny. Is presented informally as Malakoff granite [?].|1505 +/- 5 Ma.|Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite|
30704|Malakoff Granite|69056|5|Briefly described|p4, p14 Tb.3, p18, p23, p28, p56|Calymmian|Calymmian|See also Time-Space plot sheet. Large intrusion dominating the southern section of Constantine Domain. Modelling values listed. Post-dates the Isan Orogeny.|1505 +/- 5 Ma (Page and Sun, 1998).|Williams Supersuite.|||Pink medium-grained granite with minor granodiorite; mostly undeformed.|
30704|Malakoff Granite|69549|6|Mentioned|p95|Calymmian|Calymmian|Shown as Malakoff granite.|1505+/-5 Ma.|||||16-NOV-16
30704|Malakoff Granite|69591|5|Briefly described|p59||||1505 +/- 5 Ma (Page and Sun, 1998).|Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70353|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70354|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70532|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Pink, medium-grained biotite granite; minor granodiorite.|
30704|Malakoff Granite|70574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Constantine Domain.||Williams Supersuite|||Pink medium grained, biotite granite; minor granodiorite.|
30704|Malakoff Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1505+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30704|Malakoff Granite|72799|6|Mentioned|p1, p32|||Williams/Naraku Batholiths.||||||
30704|Malakoff Granite|72949|6|Mentioned|p35|Calymmian|Calymmian|Mount Isa Inlier, Western Fold Belt.||||||
30704|Malakoff Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1505 +/- 5 Ma|||||
27187|Malbon Group|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Includes: Mitakoodi Quartzite, Marraba Volcanics.||||||
27187|Malbon Group|22460|5|Briefly described|p445|||||||||
27187|Malbon Group|22461|5|Briefly described|p480|||Also see p463 and Fig 1 p464. Overlain by Mary Kathleen Group.  Underlain by Tewinga Group.||||||06-FEB-07
27187|Malbon Group|22483|6|Mentioned|Table 2 p416.|||||||||
27187|Malbon Group|22522|6|Mentioned|p330,Fig2p332|Statherian|Statherian|Max Age: 1780 Ma; Min Age: 1760 Ma||||||
27187|Malbon Group|23069|5|Briefly described|p775 (fig 1)|||||||||
27187|Malbon Group|23070|5|Briefly described|p769 (fig 1)||Statherian|||||||
27187|Malbon Group|23192|6|Mentioned|Fig.2|||||||||
27187|Malbon Group|23458|6|Mentioned|p119|||Northern boundary of this pluton is in contact with Levian Granite.  Dominantly quartzite metasediments.||||||27-AUG-07
27187|Malbon Group|23613|5|Briefly described|p724 Fig. 1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27187|Malbon Group|23962|5|Briefly described|p1214|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Age: 1780-1760Ma.||||||
27187|Malbon Group|23966|5|Briefly described|p1308|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
27187|Malbon Group|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Unconformably overlain by the Mary Kathleen Group.||||||
27187|Malbon Group|24254|6|Mentioned|p22|||||||||
27187|Malbon Group|24255|5|Briefly described|p32, Fig.1|||Geological Province: Eastern Succession, Mount Isa Block.||||||
27187|Malbon Group|24256|6|Mentioned|p54|||Geological Province: Mount Isa Block.||||||
27187|Malbon Group|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
27187|Malbon Group|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27187|Malbon Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Contains the Mitakoodi Quartzite.||||||25-AUG-04
27187|Malbon Group|30530|2|Defined|p516|Precambrian|Precambrian|||||||
27187|Malbon Group|30531|6|Mentioned|p15|||Also mention p18 and p22.||||||15-MAR-07
27187|Malbon Group|30534|6|Mentioned|p306|||||||||
27187|Malbon Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27187|Malbon Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27187|Malbon Group|32660|5|Briefly described|Table 5|||||||||
27187|Malbon Group|32959|6|Mentioned|Fig.21|||||||||
27187|Malbon Group|33111|6|Mentioned|p5|||||||||
27187|Malbon Group|33900|6|Mentioned|p4|||||||||
27187|Malbon Group|35074|6|Mentioned|Fig.2|||||||||
27187|Malbon Group|35295|6|Mentioned|p601|||||||||
27187|Malbon Group|35950|6|Mentioned|p305|||||||||
27187|Malbon Group|37462|4|Described|Table4.VII|||||||||
27187|Malbon Group|37565|5|Briefly described|p2|||See also Fig.5||||||
27187|Malbon Group|37568|4|Described|p81|||See also Fig.5||||||
27187|Malbon Group|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27187|Malbon Group|37862|6|Mentioned|p587|||||||||
27187|Malbon Group|38234|6|Mentioned|p104|||||||||
27187|Malbon Group|38275|6|Mentioned|p181|||||||||
27187|Malbon Group|38276|6|Mentioned|Fig.1|||||||||
27187|Malbon Group|38278|6|Mentioned|Fig.1|||||||||
27187|Malbon Group|38350|6|Mentioned|p5|||||||||
27187|Malbon Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27187|Malbon Group|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Overlies the Argylla Formation.||||||25-AUG-04
27187|Malbon Group|39202|6|Mentioned|Fig.2|||||||||
27187|Malbon Group|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27187|Malbon Group|39445|6|Mentioned|p40|||Correlation||||||
27187|Malbon Group|39496|6|Mentioned|p5|||||||||
27187|Malbon Group|39622|6|Mentioned|Fig.2|||||||||
27187|Malbon Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27187|Malbon Group|40840|6|Mentioned|Map legend|||||||||
27187|Malbon Group|41306|4|Described|p5|||||||||
27187|Malbon Group|41464|6|Mentioned|Map legend|Proterozoic||||||||
27187|Malbon Group|41556|6|Mentioned|Map legend|Proterozoic||||||||
27187|Malbon Group|41568|4|Described|p5|||||||||
27187|Malbon Group|41791|6|Mentioned|p248|||||||||
27187|Malbon Group|41978|6|Mentioned|p492|||||||||
27187|Malbon Group|42565|4|Described|Table 1 P5, P3|||||||||
27187|Malbon Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes Marraba Volcanics and  Mitakoodi Quartzite||||||09-FEB-09
27187|Malbon Group|43620|6|Mentioned|Fig.1,p51|||||||||
27187|Malbon Group|45136|4|Described|Table 1|||||||||
27187|Malbon Group|45161|4|Described|p39|||||||||
27187|Malbon Group|45166|4|Described|p20|||||||||
27187|Malbon Group|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
27187|Malbon Group|46919|6|Mentioned|p213|||||||||
27187|Malbon Group|46962|4|Described|Table 1|||||||||
27187|Malbon Group|46995|6|Mentioned|p269|||||||||
27187|Malbon Group|46996|6|Mentioned|p273|||||||||
27187|Malbon Group|49041|5|Briefly described|Table 3|||||||||
27187|Malbon Group|50536|6|Mentioned|p10.2|||Intruded by the Williams Supersuite.||||||
27187|Malbon Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Marraba Volcanics, Mitakoodi Quartzite.||||||
27187|Malbon Group|61925|5|Briefly described|p57 Fig. 2, p65|||Includes Argylla Formation, Magna Lynn and Marraba Volcanics, Mitakoodi and Ballara Quartzites. Cut by the Arch Rock and Buka Rock Faults.  Geological Province: Leichardt Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||
27187|Malbon Group|61926|5|Briefly described|p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes Magna Lynn and Marraba Volcanics, Mitakoodi and Ballara Quartzites. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
27187|Malbon Group|63055|5|Briefly described|p12 Fig. 1|||Part of Cover Sequence 2.||||||
27187|Malbon Group|64250|6|Mentioned|p25 fig 10|||Eastern Succession, Mount Isa Inlier.||||||
27187|Malbon Group|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~1790-1720Ma. Geological Province: Mount Isa Block.||||||
27187|Malbon Group|65396|5|Briefly described|p78, p439|||Cover Sequence 2, Mount Isa Inlier.|c.1755 +/- 3 Ma.||Includes Mitakoodi Quartzite, Marraba Volcanics|Equivalent to Ballara Quartzite.||04-APR-17
27187|Malbon Group|67323|5|Briefly described|GIS attrib tbl, p16, p71-72|Proterozoic|Proterozoic|See also Solid Geology Map. Associated with clusters of Au and Ag anomalies, particularly to the SW and SE of Cloncurry; also Cu and IOGC anomalies.|||Includes Cone Creek Metabasalt Member, Marraba Volcanics,  Mitakoodi Quartzite, Mount Start Member, Timberoo Member, Wakeful Metabasalt Member,|||
27187|Malbon Group|69056|6|Mentioned|p2, Reference images sheet|Statherian|Statherian|Shown on the simplified surface and solid geology maps of the Quamby Project area.||||||
27187|Malbon Group|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Mitakoodi Quartzite, Marraba Volcanics|||
27187|Malbon Group|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Mitakoodi Quartzite, Marraba Volcanics|||
27187|Malbon Group|69591|5|Briefly described|p57|||Mitakoodi Domain, Mount Isa Province. Part of Myally Supersequence.|||Mitakoodi Quartzite, Marraba Volcanics.|||
27187|Malbon Group|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Mitakoodi Quartzite.|||
27187|Malbon Group|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Mitakoodi Quartzite.|||
27187|Malbon Group|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Marraba Volcanics, Mitakoodi Quartzite, Overhang Jaspilite.|||
27187|Malbon Group|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Marraba Volcanics, Mitakoodi Quartzite, Overhang Jaspilite.|||
27187|Malbon Group|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Mitakoodi Quartzite, Overhang Jaspilite.||Sandstone, siltstone, silicified limestone.|
27187|Malbon Group|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||Includes Overhang Jaspilite, Mitakoodi Quartzite|||
27187|Malbon Group|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.|||Includes Marraba Volcanics, Mitakoodi Quartzite and Overhang Jaspilite.|||
27187|Malbon Group|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.|||Includes Marraba Volcanics, Mitakoodi Quartzite and Overhang Jaspilite.|||
27187|Malbon Group|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as significantly older than the the Wonga-Burstall Event (c. 1740 Ma).|||Includes Marraba Volcanics. Mitakoodi Quartzite and Overhang Jaspilite|Shown as unconformably overlying Bulonga Volcanics and underlying Chumvale Breccia.|Metabasalt, amphibolite, metasandstone and schist; minor chert. Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone. Includes slate, metasiltstone, pink feldspathic sandstone and subordinate quartzose sandstone.|
27187|Malbon Group|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as significantly older than the the Wonga-Burstall Event (c. 1740 Ma).|||Includes Marraba Volcanics. Mitakoodi Quartzite and Overhang Jaspilite|Shown as unconformably overlying Bulonga Volcanics and underlying Chumvale Breccia.|Metabasalt, amphibolite, metasandstone and schist; minor chert. Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone. Includes slate, metasiltstone, pink feldspathic sandstone and subordinate quartzose sandstone.|
27187|Malbon Group|73553|6|Mentioned|p177 Tb.5.9.1|||Contains mafic intrusive rocks.||||||
28713|Maleny Basalt|36806|5|Briefly described|p131-133|Miocene|Eocene|Succession of mafic flows.Maximum thickness 280m, cropping out over 200 sq km. K-Ar date of 25.2 m.y. from megacrystal andesine and anothoclase in one of the younger flows|21-34 my total rock K-Ar. 25.2 my from young flow|||||24-SEP-22
28713|Maleny Basalt|38310|6|Mentioned|p237|||||||||
76899|Mallee Gap Tonalite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event||Williams Supersuite|||Medium to coarse grained, strongly to unfoliated tonalite and albitite|
76899|Mallee Gap Tonalite|69591|5|Briefly described|p59||||1552 +/- 42 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.|||Medium- to coarse-grained, strongly to unfoliated tonalite and albite.|
76899|Mallee Gap Tonalite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Medium to coarse-grained, strongly foliated to unfoliated tonalite and albitite.|05-MAY-16
76899|Mallee Gap Tonalite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium-coarse grained, strongly foliated to unfoliated tonalite and albitite.|
76899|Mallee Gap Tonalite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Williams Supersuite|||Medium-coarse grained, strongly to unfoliated tonalite and albitite.|20-JAN-22
76899|Mallee Gap Tonalite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Williams Supersuite|||Medium-coarse grained, strongly-unfoliated tonalite and albitite.|
76899|Mallee Gap Tonalite|71592|5|Briefly described|Appendix A.|||Doherty-Fig Tree Gully Domain, Mount Isa Orogen. Has inherited zircons dated 1740 +/- 23 Ma; underwent Pb loss at 1552 +/- 42 Ma.|<1740 Ma.||||Tonalite.|
26312|Malmesbury Microgranite|23032|4|Described|p41||Visean|Unit previously part of Oweenee Granite.||||||
26312|Malmesbury Microgranite|23422|5|Briefly described|p181, p205 Table 6.3|Early Carboniferous|Early Carboniferous|Of Oweenee Supersuite. Intrudes the Oweenee Rhyolite.||||||
26312|Malmesbury Microgranite|23424|5|Briefly described|Fig 8.4||Carboniferous|||||||
26312|Malmesbury Microgranite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
26312|Malmesbury Microgranite|23513|5|Briefly described|Map legend||Early Carboniferous|Palaeozoic Intrusive No. 164. I-Type.||||||
26312|Malmesbury Microgranite|23893|5|Briefly described|p9 Fig. 4|Early Carboniferous|Early Carboniferous|||||||
26312|Malmesbury Microgranite|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin.||||||
26312|Malmesbury Microgranite|24613|5|Briefly described|p6 Fig. 3|Early Carboniferous|Early Carboniferous|Geological province: Burdekin Basin.||||||07-FEB-11
26312|Malmesbury Microgranite|41735|2|Defined|p287|Carboniferous?||||||||
26312|Malmesbury Microgranite|41774|6|Mentioned|p32|||Formerly Oweenee Granite||||||
26312|Malmesbury Microgranite|42054|6|Mentioned|p272|||||||||
26312|Malmesbury Microgranite|42295|6|Mentioned|Fig.2 P5|||||||||
26312|Malmesbury Microgranite|42690|5|Briefly described|map legend|Carboniferous||||||||
26312|Malmesbury Microgranite|42692|5|Briefly described|map legend|Carboniferous||||||||
26312|Malmesbury Microgranite|42933|3|Fully described|p217|||||||||
26312|Malmesbury Microgranite|43095|3|Fully described|p37|||||||||
26312|Malmesbury Microgranite|43259|4|Described|Appendix 1,p26.||Early Carboniferous|Early Carboniferous?.||||||
26312|Malmesbury Microgranite|43589|5|Briefly described|p21|||Has contact with Baumans Camp Granite.||||||23-APR-08
26312|Malmesbury Microgranite|63154|5|Briefly described|p285 Fig. 5|Early Carboniferous|Early Carboniferous|Geological province: Charters Towers Province. Presented informally as Malmesbury microgranite.||||||
26312|Malmesbury Microgranite|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province, Clarke River Basin.|||||Pink, coarsely porphyritic hornblende microgranite, with feldspar phenocrysts to 3 cm and embayed quartz phenocrysts to 1 cm.|
26312|Malmesbury Microgranite|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province, Clarke River Basin.|||||Pink, coarsely porphyritic hornblende microgranite, with feldspar phenocrysts to 3 cm and embayed quartz phenocrysts to 1 cm.|
26312|Malmesbury Microgranite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink, coarsely porphyritic hornblende microgranite, with feldspar phenocrysts to 3 cm and embayed quartz phenocrysts to 1 cm.|
26312|Malmesbury Microgranite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Pink, coarsely porphyritic hornblende microgranite, with feldspar phenocrysts to 3 cm and embayed quartz phenocrysts to 1 cm.|
26312|Malmesbury Microgranite|68576|5|Briefly described|Q_11: p38, p40|Carboniferous|Carboniferous|Camel Creek Subprovince. Coeval with Oweenee Rhyolite. Kennedy Igneous Association. Forms hilly topography.|||||Coarsely porphyritic.|
26312|Malmesbury Microgranite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
23755|Mamberra Andesite Member|23291|4|Described|p37, p81 Tb. 3.6|Carboniferous|Devonian|Parent: Gilberton Formation. Geological Province: Georgetown Region.||||||28-MAY-15
23755|Mamberra Andesite Member|23430|5|Briefly described|p509|||Gilbert Formation. Gilberton Basin.||||||
23755|Mamberra Andesite Member|39917|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian-Early Carboniferous||||||
23755|Mamberra Andesite Member|40542|6|Mentioned|p97|||||||||
23755|Mamberra Andesite Member|50199|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Gilberton Formation.||||||
23755|Mamberra Andesite Member|68353|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.||Unit in Gilberton Formation.|||Grey to green, aphyric to sparsely porphyritic pyroxene-hornblende andesite(?).|
23755|Mamberra Andesite Member|69591|5|Briefly described|p103|||SE edge of the Newcastle Range.||Gilberton Formation.|||Extensively altered andesitic lavas.|
75639|Mamelon Quartz Monzodiorite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Grey to dark grey, fine to medium-grained, uneven-grained to slightly porphyritic hornblende-biotite and biotite-hornblende quartz monzodiorite; partly to extensively recrystallised, with a well-developed foliation.|
28718|Manaman Granodiorite|23052|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
28718|Manaman Granodiorite|23161|4|Described|p41 table5|Early Permian|Late Carboniferous|Rb/Sr Age: 308+/-3 Ma.||||||
28718|Manaman Granodiorite|42701|2|Defined|p89|Late Carboniferous||Rb/Sr 308 +/- 3Ma. Reserved as Mount Manaman Granodiorite.||||||
28718|Manaman Granodiorite|43775|6|Mentioned|p28||Carboniferous|||||||
28718|Manaman Granodiorite|44245|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
28718|Manaman Granodiorite|60659|4|Described|p13, p17|Late carboniferous|Late Carboniferous|Rocks include biotite-hornblende granodiorite to tonalite and granite. Intruded into and metamorphosed Mount Coolon Andesite. Age: 308+/-3Ma.||||||07-FEB-11
28718|Manaman Granodiorite|69593|5|Briefly described|p495|Permian|Late Carboniferous|Burdekin Falls Subprovince.|~297-290 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
28718|Manaman Granodiorite|70740|5|Briefly described|p127|||Outcrop and geophysical characteristics and distribution are briefly discussed. |308+/- 3 Ma (Rb-Sr, Hutton et al., 1998)|||Intrudes the Anakie Metamorphic Group and Mount Coolon Andesite.|Biotite-hornblende granodiorite and granite quartz-feldspar porphyry.|
28718|Manaman Granodiorite|73035|5|Briefly described|Map legend|Permian|Permian||||||Biotite hornblende granodiorite, granite, quartz-feldspar porphyry.|
36572|Mandalee granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 271.  I-Type.||||||
23760|Maneater Granodiorite|23423|5|Briefly described|p315 Table 7.4||Early Permian|Also see p244. Unit has not been isotopically dated. Lags Supersuite.||||||
23760|Maneater Granodiorite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Of Lags Supersuite.||||||
23760|Maneater Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 428. A-Type.||||||
23760|Maneater Granodiorite|23616|6|Mentioned|p80|||||||||
23760|Maneater Granodiorite|42681|4|Described|p21|||||||||
23760|Maneater Granodiorite|43060|5|Briefly described|p112|||Of Lags Supersuite.||||||19-FEB-07
23760|Maneater Granodiorite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Granophyric biotie-hornblende granodiorite - pale to medium-dark grey, fine- to medium-grained, sparsely porphyritic to equigranular.||||||15-JUN-06
23760|Maneater Granodiorite|43259|4|Described|Appendix 1,p46.||Permian|||||||
23760|Maneater Granodiorite|43626|6|Mentioned|p42|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgroup.||||||
23760|Maneater Granodiorite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province.||||||
23760|Maneater Granodiorite|60425|4|Described|p47 Tb. 3, p58 Tb. 4, p79|Early Permian|Early Permian|Of Maneater Suite (Lags Sup'ste).Cuts Timber Top Volc.Subgroup. A-type, fine- to med.gr.,slightly porph.to even-gr., granophyric biotite-hornblende granodiorite - contains hypersthene +/or augite, v. rare garnet, +enclaves of arenite+granite - more lith.||||||07-FEB-11
23760|Maneater Granodiorite|62523|4|Described|p10-11, p3-4 (map/legend)|Early Permian|Early Permian|Of Yongala Volcanic Subgroup. Mainly sparsely porphyritic, med.to fine-gr.granodiorite; + less dominant,variably porph. microgranodiorite to dacite. Gently dipping portions of Maneater Granodiorite, which are probably at least 200m thick locally, are underlain and overlain by Controversy Hill Rhyolite.||||||07-APR-15
23760|Maneater Granodiorite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Lags Supersuite.|||Granophyric (garnet-hypersthene-augite-)biotite-hornblende granodiorite with inclusions of arenite and granite; pyroxene-biotite-hornblende granodiorite grading into slightly porphyritic dacite.|
23760|Maneater Granodiorite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Lags Supersuite.|||A-type.|
69317|Maneater Suite|60425|5|Briefly described|p276-7 Appdx.|Early Permian|Late Carboniferous|Of Lags Supersuite. Contains Maneater Granodiorite.  A-type granite. Lithologocal details included.||||||07-FEB-11
69317|Maneater Suite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Lags Supersuite.|Bustlem Microgranite, Maneater Granodiorite, Saint Helena Monzogranite.||A-type.|
82894|Maneroo Volcanics|73177|6|Mentioned|p1113-1114 Figs.15-16|Ordovician|Cambrian|Only in figures.||||||
79722|Maneroo volcanics|70749|5|Briefly described|p43-44, 45|Ordovician|Ordovician|New, informal name. Undercover Thomson Orogen. Also appears as Maneroo Volcanics in Fig.4. Identified in GSQ Maneroo 1; PPC Carlow 1; BEA Coreena 1; PON Muttaburra 1.|~483-473 Ma (Draper, 2006).|||Correlates with Seventy Mile Range Group.|Felsic volcanics including crystal-rich, strongly welded rhyolitic ignimbrite, shallow level rhyolitic intrusions.|18-JAN-17
79722|Maneroo volcanics|71966|5|Briefly described|p989,991-992,999|Floian|Floian|Geological province: Thomson Orogen. Informal nomenclature of Carr et al. (2014); associated with 490-460 Ma Larapinta extensional event. I-type volcanism. Intersected in drillholes GSQ Maneroo 1, BEA Cooreena 1 and PPC Carlow 1, and samples analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Weighted mean 206Pb/238U ages of 472.0+\-3.6 Ma (sample 1682888), weighted mean 206Pb/238U age of 477.8+\-3.5 Ma (sample 1682890) and 479.7+\-7.4 Ma (sample 1574653). Age of 472+\-3.6 Ma interpreted as crytallisation age. Similar in age and lithology to exposed felsic volcanics of the Seventy Mile Range Group and Balcooma Metavolcanic Group, and confirms the presence of Early Ordovician magmatic Thomson Orogen rocks below the Adavale Basin (Draper, 2006).|472.0+\-3.6 Ma (crystallisation)|||||
40125|Mannersley Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgma].  Pink to grey porphyritic biotite-hornblende quartz microdiorite with abundant secondary biotite along joints.||||||
36421|Manor Creek Microgranite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p26. Kennedy Province.||||||
36421|Manor Creek Microgranite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36421|Manor Creek Microgranite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
29340|Manumbar Metamorphics|22845|2|Defined|p58-61,63,4,78||Carboniferous|Contains 3 lithological subdivisions.||||||
29340|Manumbar Metamorphics|22846|6|Mentioned|p9,10,12|Carboniferous|Devonian|||||||
29340|Manumbar Metamorphics|23251|6|Mentioned|p29|||Named by Don Chak & others (1995). Of Claddagh-Manumbar Assemblage.||||||
29340|Manumbar Metamorphics|23608|5|Briefly described|p50 Fig 1, p56|Carboniferous|Devonian|||||||
29340|Manumbar Metamorphics|23799|6|Mentioned|p123|||Included in the "Claddagh-Manumbar Assemblage" of Little (1993).  Geological Province: North D'Aguilar Subprovince.||||||
29340|Manumbar Metamorphics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
29340|Manumbar Metamorphics|44923|5|Briefly described|Map Legend||Carboniferous|||||||
29340|Manumbar Metamorphics|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
29340|Manumbar Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
29340|Manumbar Metamorphics|68679|5|Briefly described|p322, p324-326, p331-332|Pennsylvanian|Pennsylvanian|Part of the Claddagh-Manumber Assemblage in the North D'Aguilar Subprovince. Includes metasediments and metavolcanics peripheral to the Claddagh, Gallangowan and Karandah Granodiorites. Synchronous with Wide Bay Creek Gneiss. Some suggested correlations mentioned.||||Thrust over Amamoor beds. Contains granitic veinlets of Wide Bay Creek Gneiss.|Amphibolite, fine- to medium-grained with strong mineral lineation; greenschist, fine-grained, typically cut by numerous thin, epidote-rich bands and veins; both metamorphosed mafic lavas; phyllite (metapelite), strongly lineated. Granitic veinlets.|
75735|Many Peaks Granite|67874|5|Briefly described|p1-3, p21-25, p50|Permian|Permian|These rocks were formerly part of Castletower Granite. SHRIMP U-Pb zircon magmatic crystallisation age.|268.1 +/- 1.8 Ma (SHRIMP U-Pb zircon).||||Granite; includes a fine- to medium-grained, equigranular, miarolitic, leucocratic, hornblende-biotite syenogranite.|06-NOV-15
75735|Many Peaks Granite|68679|5|Briefly described|p337, p410, p421-422, p423 Fig.5.91,p470|||Gayndah-Gladstone belt. Very extensive unit. Formerly mapped as Castletower Granite. Forms high-relief topography.|268.1 +/- 1.7 Ma (SHRIMP: Cross et al., 2012).|||Adjacent to and intimately associated with Jackass Gabbro.|Pink, fine- to medium-grained, leucocratic (biotite) arfvedsonite and (arfvedsonite-)biotite syenogranite to monzogranite; commonly granophyric. A-type.|
75735|Many Peaks Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|268+/-1.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Syenogranite.|
75735|Many Peaks Granite|73197|6|Mentioned|p476 Fig.7, p477|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase.|269 or 268 Ma U-Pb||||Granitoids.|
75735|Many Peaks Granite|73450|6|Mentioned|p9|late Permian|late Permian|||||Intruded by Castletower Granite.||
31448|Maramungee Suite|24197|5|Briefly described|p19|||Type example of the Maramungee Association - type example is the Maramungee Granite - predominantly a trondhjemite. Geological province: Mount Isa Inlier.||||||07-FEB-11
31448|Maramungee Suite|50100|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|||||||15-MAR-07
31448|Maramungee Suite|50536|5|Briefly described|p1.5, 9.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Age: 1545Ma.||||||
31448|Maramungee Suite|50537|6|Mentioned|p1.1, 4.1|||Geological Province: Mount Isa Inlier.||||||
31448|Maramungee Suite|64249|5|Briefly described|p92, p103|Mesoproterozoic|Mesoproterozoic|Age: 1526-1555Ma. Geological Province: Mount Isa Inlier. Granites of this Suite are mentioned on p103.||||||22-APR-09
31448|Maramungee Suite|67323|5|Briefly described|GIS attrib tbl, p21, p107|||See also Solid Geology Map. Soldiers Cap Domain.|Intruded between ~1550 - 1520 Ma.||Includes Maramungee Tonalite, Minya Pegmatite.|Intrudes Soldiers Cap Group and Staveley Formation.||
31448|Maramungee Suite|69056|5|Briefly described|p5|||Intruded over a protracted period.|~1550-1500 Ma.||||Granitic rocks.|
31448|Maramungee Suite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.|||Dingo Prospect Skarn.|||05-MAY-16
31448|Maramungee Suite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Dingo Prospect Skarn.|||
31448|Maramungee Suite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Dingo Prospect Skarn, Maramungee Tonalite.|||
31448|Maramungee Suite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||Includes Maramungee Tonalite, Dingo Prospect Skarn.|||
79463|Maramungee Tonalite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event. See also reference to the (superseded) Maramungee Granite (p21).||Maramungee Suite|||Fine to pegmatitic leucocratic biotite granite, granodiorite, and tonalite; foliated to massive|
79463|Maramungee Tonalite|69591|5|Briefly described|p59|||Maramungee area.|1545 +/- 11 Ma (Page and Sun, 1998).||||Fine to pegmatitic leucocratic biotite granite to tonalite; foliated to massive.|
79463|Maramungee Tonalite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Maramungee Suite|||Fine to pegmatitic leucocratic biotite granite, granodiorite and tonalite; foliated to massive.|20-JAN-22
79463|Maramungee Tonalite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.||Maramungee Suite|||Fine-pegmatitic leucocratic biotite granite, granodiorite and tonalite; foliated-massive.|
69454|Maranoa Surface|61198|5|Briefly described|p18 Tb. 3|Quaternary|Quaternary|Fan sediments. Age is early quaternary. See also Maranoa surface.||||||
69454|Maranoa Surface|61200|6|Mentioned|p9 Fig. 3, p47|||Referred to in older literature as Maranoa Fan. Largely derived from and overlies the Griman Creek Formation.  See also Maranoa surface.||||||13-JUL-05
69454|Maranoa Surface|69599|6|Mentioned|p586|Quaternary|Quaternary|Lower Balonne area.||||||
32045|Marble Waterhole beds|23468|5|Briefly described|Table 1 p 296|Givetian|Givetian|also see  p 303||||||
32045|Marble Waterhole beds|24491|4|Described|p16|Middle Devonian|Middle Devonian|Supersedes part of Kroombit beds.||||||
32045|Marble Waterhole beds|24615|5|Briefly described|CD|Middle Devonian|Middle Devonian|[Dm].  Granule to cobble andesitic breccia, fine to medium quartz-bearing lithofeldspathic sandstone, siltstone, minor felsic ignimbrite; granule to pebbly polymictic limestone-bearing breccia; locally porphyritic and amygdaloidal andesite; some limestone||||||
32045|Marble Waterhole beds|50197|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32045|Marble Waterhole beds|50214|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Overlain by Lochnbar Formation.||||||17-MAY-04
32045|Marble Waterhole beds|60282|5|Briefly described|p8|Middle Devonian|Middle Devonian|Previously mapped as part of the Krommbit beds.  Considered to be part of the Yarrol Project team's Mount Morgan Stratigraphic Assemblage.  Age is Givetian.  Overlain by Lochenbar beds with a fault boundary. Geological Province: Yarrol Province.||||||
32045|Marble Waterhole beds|61730|5|Briefly described|p994 Fig.1, p1000|Middle Devonian|Late Silurian|Previously part of the Kroombit beds. Consists of sandstone and conglomerate containing mainly dacitic clasts; thick fossiliferous limestones of late Middle Devonian age dominate the lower part of the unit. Geological Province: Yarrol Province.||||||
32045|Marble Waterhole beds|63600|5|Briefly described|p900 Fig. 1|Middle Devonian|Late Silurian|||||||07-FEB-11
32045|Marble Waterhole beds|68008|2|Defined|p27, p42-48, p63-64, p66-67, p109, p131|Givetian|Givetian|See also p209, p477, p479, p568, p573, p579-580, p602, p648, p651. Originally part of the Kroombit beds (Dear, 1968; Dear et al., 1971). Forms a NW-trending belt 20 x 5 km. Named after Marble Waterhole, Kroombit Creek. The type area is in two parts (described) at Marble Waterhole; total thickness is 234m. With the Capella Creek Group, comprises the Mount Morgan Stratigraphic Assemblage. Close age and composition relationships to Ginger Creek Member (Raspberry Creek Formation). Locally intense block faulting; numerous dykes. Rich coral fauna listed. Hosts the (historic) Allen Creek, or Mount Kroombit, Cu Mine.  Structural data discussed. Micropaleontology table. Measured section diagram.||||Is overlain unconformably by Youlambie Conglomerate and Winterbourne Volcanics. Is faulted against the Lochenbar Formation and Rockhampton Group.|Generally grey-green rocks: mainly fossiliferous limestone; also feldspatholithic sandstone, granule to pebble dacitic breccia/conglomerate and dacitic to rhyolitic tuff/ignimbrite; rare andesite.|
32045|Marble Waterhole beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Craigilee, Calliope, Munbooree and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
32045|Marble Waterhole beds|68679|5|Briefly described|p312-313, p316, p338-339|Givetian|Givetian|Capella Subprovince, northern New England Orogen. Murray et al. (2012). Originally the lower part of the Kroombit beds of Dear (1968), later expanded by Dear, McKellar and Tucker (1971). Forms a NW-trending belt 20km long and up to 5km wide, from near Blue Hills to the headwaters of Kroombit Creek where it is 234m thick. Has lithological and geochemical similarities with Ginger Creek Member (Raspberry Creek Formation). Fossil fauna includes at least 20 species of corals.||||Is overlain unconformably by Youlambie Conglomerate and Winterbourne Volcanics. Is faulted against the Lochenbar Formation and Rockhampton Group.|Thick-beddded, fossiliferous limestone with locally abundant volcanic quartz and feldspar grains and ooliths; also feldspatholithic sandstone, granule to pebble dacitic conglomerate, dacitic to rhyolitic tuff/ignimbrite and rare andesite.|
32045|Marble Waterhole beds|73143|6|Mentioned|p17|Givetian|Givetian|Contains rugose coral Nardophyllum immanum (Blake, 2010).||||||
69320|Mareeba Suite|60425|5|Briefly described|p81 Tb. 5, p274-5 Appdx. 1|Early Permian|Early Permian|Of the Whypalla Supersuite. Contains Mareeba Granite. Age: 278Ma, 279Ma (Rb-Sr). S-type.||||||07-FEB-11
69320|Mareeba Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Mareeba Granite.|||
81010|Marker Seam|68679|5|Briefly described|p398|Late Triassic|Late Triassic|Informal subdivision of the coal measures (Reid 1945, 1947; Dear, McKellar & Tucker 1971; Flood 1985) recognised a basal conglomerate followed above by the Bottom, Sawmill, Callide and Marker seams.||Callide Coal Measures.||||30-APR-19
36554|Marlborough Pocket Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 218.  I-Type.||||||
36554|Marlborough Pocket Granodiorite|69593|5|Briefly described|p494, p513|Permian|Late Carboniferous|Paluma, Burdekin Falls Subprovinces, Kennedy Igneous Association. Charters Towers-Townsville area. Sm-Nd isotope data tabulated.|280 Ma.|Leichhardt Suite.|||I-type.|
23765|Maronan Supergroup|22467|5|Briefly described|Fig 2 p431.|||||||||
23765|Maronan Supergroup|22483|4|Described|p414|||also fig 1 p415.||||||
23765|Maronan Supergroup|22513|6|Mentioned|p373|||||||||
23765|Maronan Supergroup|22514|4|Described|p389-390,394|Statherian|Statherian|Origin of name: Beardsmore et al. 1988. Max Age: 1670 Ma; Min Age: 1620 Ma.||||||18-JAN-07
23765|Maronan Supergroup|22522|5|Briefly described|p330,335-338||Statherian|||||||
23765|Maronan Supergroup|22667|6|Mentioned|P235|||||||||
23765|Maronan Supergroup|22735|5|Briefly described|p281,2|Calymmian|Statherian|Contains Soldiers Cap Group.||||||18-JAN-07
23765|Maronan Supergroup|22956|6|Mentioned|p146,8,150||Proterozoic|||||||
23765|Maronan Supergroup|22958|5|Briefly described|p121||Statherian|||||||
23765|Maronan Supergroup|22963|6|Mentioned|p67||Paleoproterozoic|||||||07-NOV-08
23765|Maronan Supergroup|23068|5|Briefly described|p783|||||||||
23765|Maronan Supergroup|23192|6|Mentioned|Fig.2|||||||||
23765|Maronan Supergroup|23193|5|Briefly described|Fig.1|Statherian||Age: <1680Ma.||||||
23765|Maronan Supergroup|23471|5|Briefly described|p110 Fig 2||Statherian|Age: <1655 Ma. Geological Province: Mount Isa Block.||||||
23765|Maronan Supergroup|23610|5|Briefly described|p876 Fig 1|Paleoproterozoic|Paleoproterozoic|Age: <1680 Ma.||||||07-NOV-08
23765|Maronan Supergroup|23613|6|Mentioned|p724 Fig. 1|Paleoproterozoic|Paleoproterozoic|Informal name||||||07-NOV-08
23765|Maronan Supergroup|23957|6|Mentioned|p1124|||||||||
23765|Maronan Supergroup|23960|6|Mentioned|p1181 Fig. 1|Proterozoic|Proterozoic|Geological Province: Mt Isa Inlier. Age: 1680Ma.||||||
23765|Maronan Supergroup|23962|5|Briefly described|p1215 Fig. 2|||Geological Province: Mount Isa Inlier.||||||
23765|Maronan Supergroup|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
23765|Maronan Supergroup|23970|6|Mentioned|p1391 Fig.1|||Geological Province: Mount Isa Inlier||||||
23765|Maronan Supergroup|23975|6|Mentioned|p1464|Proterozoic|Proterozoic|Informal name - refer to Maronan Supergroup.||||||02-MAR-05
23765|Maronan Supergroup|24255|5|Briefly described|p32 Fig.1|||Geological Province: Eastern Succession, Mount Isa Block.||||||
23765|Maronan Supergroup|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
23765|Maronan Supergroup|24462|4|Described|p296|||Geological Province: Mount Isa Block.||||||
23765|Maronan Supergroup|41791|6|Mentioned|p266|||||||||
23765|Maronan Supergroup|41978|3|Fully described|Table 1 P492|||||||||
23765|Maronan Supergroup|42054|6|Mentioned|p272|||||||||
23765|Maronan Supergroup|42556|4|Described|p7|||||||||
23765|Maronan Supergroup|42755|5|Briefly described|p4|||||||||
23765|Maronan Supergroup|43614|6|Mentioned|p17|||||||||
23765|Maronan Supergroup|43616|6|Mentioned|p2|||||||||
23765|Maronan Supergroup|44195|6|Mentioned|p349|||Of Beardsmore et al. 1988||||||
23765|Maronan Supergroup|50100|6|Mentioned|p68|||Comprises the Soldiers Cap and Fullarton River Groups.||||||
23765|Maronan Supergroup|50125|5|Briefly described|p85|||Informal name of Beardsmore et al. (1988). Geological Province: Eastern Succession, Mount Isa Inlier.||||||
23765|Maronan Supergroup|50547|5|Briefly described|p1215||Statherian|Age: 1680-1660 Ma. Contains Fullarton River Group. In Eastern Fold Belt,  Mount Isa Inlier.||||||18-JAN-07
23765|Maronan Supergroup|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1700-1650Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
23765|Maronan Supergroup|61924|6|Mentioned|p42, p43 Fig.2|||Of Beardesmore et al 1998. Age: ~1670-1610 Ma.||||||
23765|Maronan Supergroup|61927|5|Briefly described|p92 Fig.1, p93|||Informal collective term used in this study to include Soldiers Cap Group and Kuridala Formation. Geological Province: Mount Isa Inlier.||||||
23765|Maronan Supergroup|61929|5|Briefly described|p125|||Includes Soldiers Cap and Fullarton River Groups. See also p129 Fig. 3. ||||||
23765|Maronan Supergroup|61936|6|Mentioned|p196|||Of Beardsmore et al (1988). Term for a coherent package of rift-related successions deposited in a deep marine environment. ||||||
23765|Maronan Supergroup|62641|6|Mentioned|p275, p288.|||Mount Isa region. Provenance correlations drawn with Nawa Domain (South Australian Craton) and Willyama Supergroup (Broken Hill region) suggest contiguity during late Paleoproterozoic.||||||
23765|Maronan Supergroup|63055|5|Briefly described|p12 Fig. 1|||Part of Cover Sequence 3.||||||
23765|Maronan Supergroup|63110|6|Mentioned|p1130|||Hosts Cannington.||||||11-JUN-08
23765|Maronan Supergroup|63593|6|Mentioned|p290. |||Cloncurry district, Mount Isa Inlier. An apparently conformable sequence c.10 km thick.|||||Terrigenous and volcaniclastic sediments and bimodal volcanics.|
23765|Maronan Supergroup|64250|4|Described|p12-15|||Of Beardsmore et al.(1988) to 'group'  their revised Fullarton River and Soldiers Cap Groups. They suggested it formed in the first volcanosedimentary cycle, at about 1890-1810 Ma, of the Mount Isa Inlier; this is contradicted by geochronology herein. Laing and Beardsmore (1986) and Laing (1990) suggested it was an allochthonous terrane, overthrust from the east. The authors argue that usage of this term is not justified as presently defined.|1675-1650 Ma||Fullarton River Group, Soldiers Cap Group.|||19-MAR-18
23765|Maronan Supergroup|64252|5|Briefly described|p71|||Defined by Beardsmore et al. (1988). Includes Kuridala Formation and Fullarton River Group.||||||
23765|Maronan Supergroup|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: between ~1680-1610Ma. Geological Province: Mount Isa Block.||||||
23765|Maronan Supergroup|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
23765|Maronan Supergroup|65396|6|Mentioned|p78, p176-178, p182|Orosirian|Orosirian|Of Beardsmore et al. (1988), who included the Soldiers Cap Group and their Fullarton River Group as a conformable sequence. Cover Sequence 3, Mount Isa Inlier. They suggested a depositional age of 1890-1810 Ma. More recent age determinations show a depositional age range between c.1675-1650 Ma.|||Includes Soldiers Cap Group, Fullarton River Group.|||
23765|Maronan Supergroup|66800|5|Briefly described|p928, p933.|||Eastern Fold Belt, Mount Isa Inlier. Laing (1990) proposed a temporal correlation between this unit and Etheridge and Willyama Groups; grouped into Diamantina Orogen on basis of broadly similar sedimentation, orogeny and cratonisation.|||Includes Soldiers Cap Group.|||
28725|Maroochydore Diorite|40245|6|Mentioned|Fig.4|||||||||
28725|Maroochydore Diorite|40954|6|Mentioned|p132|||||||||
28725|Maroochydore Diorite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
23768|Marquis Rhyolite|23291|4|Described|p42, p91 Tb. 3.9|Late Carboniferous|Late Carboniferous|Thickness: 150m. Included in the Cumberland Range Volcanic Group for ease of description. Geological Province: Georgetown Region.||||||29-MAY-15
23768|Marquis Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V13. Assumed to be I-Type.||||||
23768|Marquis Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23768|Marquis Rhyolite|40542|6|Mentioned|p97|||||||||
23768|Marquis Rhyolite|40860|6|Mentioned|Fig.1|||||||||
23768|Marquis Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|||||||
23768|Marquis Rhyolite|43740|3|Fully described|p23|||||||||
23768|Marquis Rhyolite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||||||
23768|Marquis Rhyolite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
23768|Marquis Rhyolite|50210|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23768|Marquis Rhyolite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of the Cumberland Range Volcanic Group.||||||
23768|Marquis Rhyolite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron.||Unit in Cumberland Range Volcanic Group.|||Cream to purple, sparsely porphyritic rhyolite.|
23768|Marquis Rhyolite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Green, cream or purple crystal-poor rhyolitic ignimbrite with very abundant lithic clasts.|
23768|Marquis Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Green cream or purple crystal-poor rhyolitic ignimbrite with very abundant lithic clasts.|
23768|Marquis Rhyolite|68415|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Includes 2 unnamed units.|||||Cream to purple, sparsely porphyritic rhyolite lava; green, cream, or purple crystal-poor rhyolitic ignimbrite with very abundant lithic clasts.|
29330|Martin Creek Microgranite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes Mount Cardwell and Saucebottle Granites; intruded by Sheba, California, Kitchener, Ootann Granites. Geological Province: Georgetown Region.||||||20-AUG-15
29330|Martin Creek Microgranite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
29330|Martin Creek Microgranite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29330|Martin Creek Microgranite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
29330|Martin Creek Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 373. I-Type.||||||
29330|Martin Creek Microgranite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29330|Martin Creek Microgranite|23624|4|Described|p13|Permian|Carboniferous|Parent: Ootann Supersuite.||||||01-JUL-15
29330|Martin Creek Microgranite|43083|5|Briefly described|p255|||Of Ootann Supersuite. I-type. Lithology included.||||||01-JUL-15
29330|Martin Creek Microgranite|43087|2|Defined|p35|Late Carboniferous||Of Ootann Supersuite. Reserved as Martin Creek Adamellite.||||||
29330|Martin Creek Microgranite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
29330|Martin Creek Microgranite|60425|4|Described|p280-1 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. Fine- to medium-grained biotite granite; leucocratic; associated with Mo mineralisation in the NW; molybdenite is mainly in quartz veins and adjacent aplitic granite.||||||01-JUL-15
29330|Martin Creek Microgranite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White, fine- to very fine-grained syenogranite and monzogranite.|
29330|Martin Creek Microgranite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White, fine- to very fine-grained syenogranite and monzogranite.|
29330|Martin Creek Microgranite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to white, fine-grained, slightly porphyritic, leucocratic biotite granite; cut by numerous closely spaced joints.|
40126|Marvel Creek Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgmc].  Dark grey, fine- to medium-grained gabbro and diorite.||||||
40126|Marvel Creek Gabbro|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
40126|Marvel Creek Gabbro|65388|3|Fully described|p325, p236, p237, p238,  p301|Early Triassic|Early Permian|Reverse polarisation contrasts with Glencoe Gabbro & may suggest early Permian age. Mainly dark grey, medium-grained olivine gabbro, altered leucogabbro, and fine to medium-grained hornblende-plagioclase diorite. The presence of olivine in places is distinctive.||||||
40126|Marvel Creek Gabbro|68679|5|Briefly described|p419|||An ovoid, ~3km long pluton in the Rawbelle Batholith. Distinguished from other gabbros by presence of olivine.|||||Gabbro and diorite.|
79119|Mary Basalt|70913|4|Described|p37-p44, 1, 11, 49, p8 fig 3, App1 map|Middle Permian|Early Permian|Gympie Province.  Said to be new name.  Shown as Mary Basalt Formation in heading p37. Named after the Mary River. Reference drill holes and a type locality are briefly mentioned. Contains narrow seams of actinolite asbestos. Ranges from 100 to 300m thick. See also p51, 52, 59, 67 fig 9, p79.||Gympie Group|Includes the Tozer Basalt Member.|Overlies the Dawn Formation, the Hall Clastics Member. Overlain by the Eldorado Clastics Member of the Rammutt Formation.|Hematised basalt flows with oxidised flow tops and pyroclastic breccias.|18-SEP-17
79119|Mary Basalt|73303|6|Mentioned|p61 Fig.2|Cisuralian|Cisuralian|New England Orogen. Gympie Terrane, southern. Vent-proximal marine volcanic setting.||||Overlies Dawn Formation, underlies Rammutt Formation.||
26018|Mary Kathleen Group|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Includes: Kuridala Formation, Corella Formation, Marimo Slate, Answer Slate, Overhang Jaspilite.||||||
26018|Mary Kathleen Group|22460|4|Described|p446-447|||||||||
26018|Mary Kathleen Group|22461|5|Briefly described|p463|||Also see p465. Overlies the  Malbon Group.||||||
26018|Mary Kathleen Group|22465|5|Briefly described|p934|||||||||
26018|Mary Kathleen Group|22468|5|Briefly described|p 17|Statherian|Statherian|Age: ~1750Ma.||||||15-MAR-07
26018|Mary Kathleen Group|22483|4|Described|p414|||also fig 1 p415.||||||
26018|Mary Kathleen Group|22514|6|Mentioned|Fig1p390|||||||||
26018|Mary Kathleen Group|22522|5|Briefly described|p330,335-337|Statherian|Statherian|Max Age: 1780 Ma; Min Age: 1760 Ma||||||
26018|Mary Kathleen Group|22523|6|Mentioned|p364,Fig1+2p364,365|||||||||
26018|Mary Kathleen Group|22667|6|Mentioned|P235|||||||||
26018|Mary Kathleen Group|22692|5|Briefly described|p765, Fig.2 p766|||Age of unit: 1740-1730 Ma (Page & Williams, 1988)||||||15-MAR-07
26018|Mary Kathleen Group|22735|5|Briefly described|p281,2,4,8|Statherian|Statherian|||||||
26018|Mary Kathleen Group|22958|6|Mentioned|p121||Proterozoic|||||||
26018|Mary Kathleen Group|23064|6|Mentioned|135|||Geol province Mt Isa Inlier||||||
26018|Mary Kathleen Group|23067|5|Briefly described|p793 (fig 1)|||||||||
26018|Mary Kathleen Group|23068|5|Briefly described|p784 (fig 1)|||||||||
26018|Mary Kathleen Group|23069|5|Briefly described|p775 (fig 1)|||||||||
26018|Mary Kathleen Group|23070|5|Briefly described|p769 (fig 1)||Statherian|||||||
26018|Mary Kathleen Group|23192|6|Mentioned|p385, Fig.2|||||||||
26018|Mary Kathleen Group|23193|6|Mentioned|Fig.1|Statherian||Age: ~1750Ma.||||||
26018|Mary Kathleen Group|23471|5|Briefly described|p111|Statherian|Statherian|Age: 1783-1760 Ma. Geological Province: Mount Isa Block.||||||
26018|Mary Kathleen Group|23518|5|Briefly described|p9 Fig. 3, p10|Proterozoic|Proterozoic|Geological Province: Eastern Fold Belt.||||||
26018|Mary Kathleen Group|23519|5|Briefly described|p110 Table 1|Mesoproterozoic|Mesoproterozoic|Geological Province: Tommy Creek Block.||||||
26018|Mary Kathleen Group|23610|5|Briefly described|p876 Fig 1|Paleoproterozoic|Paleoproterozoic|Age: ~1750 Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
26018|Mary Kathleen Group|23613|6|Mentioned|p724 Fig. 1|||||||||
26018|Mary Kathleen Group|23901|6|Mentioned|p1685|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
26018|Mary Kathleen Group|23960|6|Mentioned|p1181 Fig. 1|||Geological Province: Mt Isa Inlier.||||||
26018|Mary Kathleen Group|23962|5|Briefly described|p1214|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Age: 1780-1760Ma.||||||
26018|Mary Kathleen Group|23966|5|Briefly described|p1308|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
26018|Mary Kathleen Group|23970|5|Briefly described|p1391 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1.78-1.76Ga||||||07-NOV-08
26018|Mary Kathleen Group|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Age: 1746-1725Ma||||||
26018|Mary Kathleen Group|23973|5|Briefly described|p1436 Fig. 1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
26018|Mary Kathleen Group|23974|6|Mentioned|p1451 Fig. 1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
26018|Mary Kathleen Group|23975|5|Briefly described|p1464|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Age: 1780-1760Ma.||||||15-MAR-07
26018|Mary Kathleen Group|24254|6|Mentioned|p19 Fig. 2|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
26018|Mary Kathleen Group|24255|5|Briefly described|p30, p32 Fig.1|Statherian|Statherian|Geological Province: Eastern Succession, Mount Isa Block. Age: Hornfels and skarn 1750-1730 Ma; calc-silicate rocks, marble, pelite ~1760Ma.||||||
26018|Mary Kathleen Group|24256|6|Mentioned|p52|||Geological Province: Mount Isa Block.||||||
26018|Mary Kathleen Group|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
26018|Mary Kathleen Group|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
26018|Mary Kathleen Group|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26018|Mary Kathleen Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
26018|Mary Kathleen Group|30530|6|Mentioned|p515|||See also p516.||||||20-JUL-20
26018|Mary Kathleen Group|30531|2|Defined|p22|Precambrian|Precambrian|||||||
26018|Mary Kathleen Group|30532|6|Mentioned|p113|||||||||
26018|Mary Kathleen Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26018|Mary Kathleen Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26018|Mary Kathleen Group|32660|4|Described|Table 5|||||||||
26018|Mary Kathleen Group|32959|6|Mentioned|p31|||||||||
26018|Mary Kathleen Group|33111|6|Mentioned|p5|||||||||
26018|Mary Kathleen Group|33900|6|Mentioned|p4|||||||||
26018|Mary Kathleen Group|35074|6|Mentioned|Fig.2|||||||||
26018|Mary Kathleen Group|35295|6|Mentioned|p603|||||||||
26018|Mary Kathleen Group|35388|6|Mentioned|Fig.10|||||||||
26018|Mary Kathleen Group|35495|6|Mentioned|p341|||||||||
26018|Mary Kathleen Group|35536|6|Mentioned|p25|||||||||
26018|Mary Kathleen Group|35950|6|Mentioned|p305|||||||||
26018|Mary Kathleen Group|36052|4|Described|p419|||See also Fig.2.||||||
26018|Mary Kathleen Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26018|Mary Kathleen Group|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
26018|Mary Kathleen Group|36963|6|Mentioned|Fig.1|||||||||
26018|Mary Kathleen Group|37462|4|Described|Table4.VII|||||||||
26018|Mary Kathleen Group|37565|5|Briefly described|p2|||See also Fig.5||||||
26018|Mary Kathleen Group|37568|5|Briefly described|p83|||See also p85.||||||15-MAR-07
26018|Mary Kathleen Group|37569|6|Mentioned|p89|||||||||
26018|Mary Kathleen Group|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26018|Mary Kathleen Group|38234|6|Mentioned|p104|||||||||
26018|Mary Kathleen Group|38275|6|Mentioned|p181|||||||||
26018|Mary Kathleen Group|38276|6|Mentioned|Fig.1|||||||||
26018|Mary Kathleen Group|38278|6|Mentioned|Fig.1|||||||||
26018|Mary Kathleen Group|38350|4|Described|p11|||||||||
26018|Mary Kathleen Group|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26018|Mary Kathleen Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26018|Mary Kathleen Group|38900|6|Mentioned|p55|||||||||
26018|Mary Kathleen Group|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Answer Slate, Kuridala Formation, Doherty Formation.||||||25-AUG-04
26018|Mary Kathleen Group|39043|6|Mentioned|p9|||||||||
26018|Mary Kathleen Group|39202|6|Mentioned|Fig.2|||||||||
26018|Mary Kathleen Group|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26018|Mary Kathleen Group|39445|5|Briefly described|p42|||See also Table 2||||||
26018|Mary Kathleen Group|39496|5|Briefly described|p8|||||||||
26018|Mary Kathleen Group|39622|6|Mentioned|Fig.2|||||||||
26018|Mary Kathleen Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
26018|Mary Kathleen Group|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26018|Mary Kathleen Group|39937|5|Briefly described|p84|||||||||
26018|Mary Kathleen Group|40221|6|Mentioned|p11|||||||||
26018|Mary Kathleen Group|40623|5|Briefly described|p96|||||||||
26018|Mary Kathleen Group|40648|4|Described|p9|||||||||
26018|Mary Kathleen Group|40840|6|Mentioned|Map legend|||||||||
26018|Mary Kathleen Group|40984|4|Described|p389|||||||||
26018|Mary Kathleen Group|41069|6|Mentioned|p452|||||||||
26018|Mary Kathleen Group|41150|5|Briefly described|p1806|||||||||
26018|Mary Kathleen Group|41306|4|Described|p7|||||||||
26018|Mary Kathleen Group|41381|6|Mentioned|p323|||||||||
26018|Mary Kathleen Group|41464|6|Mentioned|Map legend|Proterozoic||||||||
26018|Mary Kathleen Group|41465|6|Mentioned|p11|||||||||
26018|Mary Kathleen Group|41556|6|Mentioned|Map legend|Proterozoic||||||||
26018|Mary Kathleen Group|41568|3|Fully described|p10|||||||||
26018|Mary Kathleen Group|41614|6|Mentioned|p1415|||||||||
26018|Mary Kathleen Group|41744|5|Briefly described|p406|||||||||
26018|Mary Kathleen Group|41791|6|Mentioned|p249|||||||||
26018|Mary Kathleen Group|41978|5|Briefly described|p491|||||||||
26018|Mary Kathleen Group|42201|6|Mentioned|p292|||||||||
26018|Mary Kathleen Group|42234|5|Briefly described|p1055|||||||||
26018|Mary Kathleen Group|42556|4|Described|p5|||||||||
26018|Mary Kathleen Group|42565|4|Described|Table 1 P5, P2|||||||||
26018|Mary Kathleen Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes Roxmere Quartzite, Staveley Formation, Marimo Slate, Overhang Jaspilite, Corella Formation and Ballara Quartzite.||||||09-FEB-09
26018|Mary Kathleen Group|42812|6|Mentioned|p65|||||||||
26018|Mary Kathleen Group|43595|5|Briefly described|p439-40|||||||||
26018|Mary Kathleen Group|43608|6|Mentioned|Fig.11,p11|||||||||
26018|Mary Kathleen Group|43614|6|Mentioned|Fig.2|||||||||
26018|Mary Kathleen Group|43615|6|Mentioned|p15|||||||||
26018|Mary Kathleen Group|43616|6|Mentioned|p4|||||||||
26018|Mary Kathleen Group|43620|6|Mentioned|Fig.1,p51|||||||||
26018|Mary Kathleen Group|43767|6|Mentioned|p890||Mesoproterozoic|||||||
26018|Mary Kathleen Group|44195|6|Mentioned|p357|||||||||
26018|Mary Kathleen Group|45136|4|Described|Table 1|||||||||
26018|Mary Kathleen Group|45161|4|Described|p24|||See also p42.||||||15-MAR-07
26018|Mary Kathleen Group|45166|4|Described|p20|||||||||
26018|Mary Kathleen Group|46801|6|Mentioned|Fig.14|||Stratigraphy||||||
26018|Mary Kathleen Group|46843|6|Mentioned|Fig.2|||||||||
26018|Mary Kathleen Group|46919|6|Mentioned|p213|||||||||
26018|Mary Kathleen Group|46960|6|Mentioned|p220|||||||||
26018|Mary Kathleen Group|46962|4|Described|Table 1|||See also Fig.3.||||||
26018|Mary Kathleen Group|47083|5|Briefly described|p10|||||||||
26018|Mary Kathleen Group|49009|6|Mentioned|p29|||||||||
26018|Mary Kathleen Group|49041|5|Briefly described|Table 2|||See also Table 3||||||
26018|Mary Kathleen Group|50081|6|Mentioned|p43|||Age: ca. 1620-1550 Ma.||||||
26018|Mary Kathleen Group|50125|6|Mentioned|p91|||||||||
26018|Mary Kathleen Group|50536|5|Briefly described|p6.3|||Intruded by Burstall Suite.  Geological Province: Mount Isa Inlier.||||||
26018|Mary Kathleen Group|50547|5|Briefly described|p1227 Fig.14||Proterozoic|Contains Corella, Doherty and Kuridala Formation. In Eastern Fold Belt,  Mount Isa Inlier.||||||
26018|Mary Kathleen Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
26018|Mary Kathleen Group|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block.||||||03-JUN-09
26018|Mary Kathleen Group|60658|5|Briefly described|p61|Proterozoic|Proterozoic|Includes Answer Slate and Staveley Formation.||||||22-JUN-16
26018|Mary Kathleen Group|60665|5|Briefly described|p1146, p1149-1151, p1156, p1163|Statherian|Statherian|Hosts Ernest Henry Cu-Au deposit. Details of ore deposits and albitisation.|1760 to 1730 Ma||Includes Corella Formation.||Calc-silicate rocks, marbles and minor pelitic and volcanic rocks. Feldspar-altered intermediate volcanic rocks. Biotite rich schists and ironstones.|
26018|Mary Kathleen Group|61928|5|Briefly described|p114|||Includes the Staveley Formation.||||||
26018|Mary Kathleen Group|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes Marraba Volcanics, Mitakoodi Quartzite, Ballara Quartzite, Corella Formation. Age: ca1800-1700Ma. ||||||07-NOV-08
26018|Mary Kathleen Group|63023|6|Mentioned|p1024 Fig. 1|||||||||
26018|Mary Kathleen Group|63055|5|Briefly described|p12 Fig. 1|||Part of Cover Sequence 2.||||||
26018|Mary Kathleen Group|64248|6|Mentioned|p36|||||||||
26018|Mary Kathleen Group|64250|4|Described|p7, p12-14|||In light of recent unequivocally young ages, the authors remove the Answer and Marimo Slates, Kuridala and Stavely Formations, and (by inference) Agate Downs Siltstone from this Group.|||Corella and Doherty Formations, Overhang Jaspilite, Chumvale Breccia, Ballara and Mitakoodi Quartzites.|||
26018|Mary Kathleen Group|64253|5|Briefly described|p151,p 152 Fig. 1, p153, p157|Paleoproterozoic|Paleoproterozoic|Age: ~1790-1720Ma. Geological Province: Mount Isa Block. Metasedimentary and metavolcanic rocks.||||||
26018|Mary Kathleen Group|65387|6|Mentioned|p3 Tb.1a||||||Includes Answer Slate and Staveley Formation.|||
26018|Mary Kathleen Group|65396|5|Briefly described|p15, p47, p78, p169, p173, p176,p178-181|Statherian|Statherian|See also p184, p217, p327, p439. Blake (1987). Mount Isa Inlier: Eastern succession, Cover Sequence 2. Younger elements of this Group (viz. Cover Sequence 3 units) have been reassigned here to the informal Young Australia Group, which has since been discontinued. |1760 - 1730 Ma||Includes Overhang Jaspilite, Corella Formation, Corella Beds, Doherty Formation, Chumvale Breccia, Ballara Quartzite, Mitakoodi Quartzite.|Conformably overlies Mitakoodi and Ballara Quartzites.|Calcsilicate rocks.|
26018|Mary Kathleen Group|67323|5|Briefly described|p71-72|Proterozoic|Proterozoic|Eastern Fold Belt, Mount Isa Inlier. Associated with clusters of Au and Ag anomalies, particularly within a 50km radius of Cloncurry; also Cu, Pb, Zn, Pb-Zn and IOCG anomalies.||||||
26018|Mary Kathleen Group|68021|6|Mentioned|p138|Paleoproterozoic|Paleoproterozoic|||||||
26018|Mary Kathleen Group|68542|6|Mentioned|p12, p13, p20 fig 6||||1755 Ma||Includes Ballara Quartzite, Corella Formation|||
26018|Mary Kathleen Group|68576|5|Briefly described|Q_2: p11-13, p20-21||||1755 Ma.||Ballara Quartzite, Corella Formation.|Overlies Myally Subgroup. Is intruded by Burstall Granite.|Includes quartzites.|
26018|Mary Kathleen Group|69222|6|Mentioned|p222 Fig.2, p223|Statherian|Statherian|Eastern and Kalkadoon-Leichhardt Fold Belts. Associated with the Myally Rift Event.|||Includes Ballara Quartzite, Corella Formation|||09-FEB-18
26018|Mary Kathleen Group|69591|5|Briefly described|p57|||Mount Isa Province. Part of the Quilalar Supersequence.|||Corella Formation, Ballara Quartzite.|||
26018|Mary Kathleen Group|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Ballara Quartzite, Corella Formation.|||
26018|Mary Kathleen Group|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Ballara Quartzite, Corella Formation.|||
26018|Mary Kathleen Group|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Corella Formation.|||
26018|Mary Kathleen Group|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Corella Formation.|||
26018|Mary Kathleen Group|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Ballara Quartzite, Corella Formation.|||
26018|Mary Kathleen Group|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Ballara Quartzite, Corella Formation.|||
26018|Mary Kathleen Group|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Ballara Quartzite, Corella Formation.|||
26018|Mary Kathleen Group|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||Includes Corella Formation, Ballara Quartzite.|||
26018|Mary Kathleen Group|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen. This age is of a provenance cluster.|1858+/-18 Ma (U-Pb zircon SHRIMP)||||Schist.|
26018|Mary Kathleen Group|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1742 +/- 6 Ma|||||
26018|Mary Kathleen Group|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.|||Includes Corella Formation and Ballara Quartzite.|Shown as equivalent to Stanbroke Sandstone, Quilalar Formation.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
26018|Mary Kathleen Group|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.|||Includes Corella Formation and Ballara Quartzite.|Shown as equivalent to Stanbroke Sandstone, Quilalar Formation.|Calcareous siltstone, sandstone and minor limestone, passing into calc-silicate granofels, commonly scapolitic, and marble; local quartzose sandstone passing into quartzite; local breccia.|
26018|Mary Kathleen Group|73137|5|Briefly described|p1, p21|||Dominated by the Corella Formation.|||Corella Formation|Unconformably underlain by Argylla Formation (Tewinga Group).||08-OCT-22
26018|Mary Kathleen Group|73529|5|Briefly described|p2 Fig.1, p4, p17|||Leichhardt Superbasin, Mary Kathleen Domain. Shallow marine depositional environment.|||Corella Formation|Unconformably underlies Mount Albert Group||
26018|Mary Kathleen Group|73553|5|Briefly described|p1-2, p5, p187|||Mary Kathleen Domain. Leichhardt Superbasin.|||Ballara Quartzite, Corella Formation|Unconformably overlies Argylla Formation|Includes felsic units.|
75652|Massey Granite|68679|5|Briefly described|p361, p366 Figs.5.53,57|Permian|Permian|Northern Connors Subprovince. Early Permian. REE plot.|290.0 +/- 1.7 Ma (U-Pb SHRIMP: Cross et al. 2012).||||Monzogranite containing abundant pale pink K-feldspar grains and small miarolitic cavities commonly lined with coarse quartz and pink K-feldspar.|
75652|Massey Granite|68901|5|Briefly described|p4, p87-p90, p146|Permian|Permian|Northern New England Orogen, Bowen Region. Forms extensive outcrops in the bed of Massey Creek.SHRIMP age is interpreted as the age of magmatic crystallisation. Petrography and SHRIMP results and analyses discussed in detail.|290 +/- 1.7 Ma (SHRIMP U-Pb)||||Pale-pink, medium-grained, slightly porphyritic, leucocratic tourmaline-muscovite-biotite monzogranite that is massive and unfoliated.|16-NOV-18
75652|Massey Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|290+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
75652|Massey Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, slightly porphyritic, leucocratic biotite monzogranite; with scattered tourmaline-rich nodules; variably and pervasively altered, with chlorite after biotite and late-stage interstitial tourmaline and muscovite.|
75652|Massey Granite|73037|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, slightly porphyritic, leucocratic biotite monzogranite; with scattered tourmaline-rich nodules; variably and pervasively altered, with chlorite after biotite and late-stage interstitial tourmaline and muscovite.|
82985|Masterson Basalt|73115|6|Mentioned|p29|Pleistocene|Pleistocene|McBride Basalt Province.|0.41 Ma|||Overlain by Wyandotte Formation.||
39155|Matchbox Range Granite|65452|6|Mentioned|p6 Fig.2, p29|Late Triassic|Late Triassic|Geochemistry briefly described.||||||
39155|Matchbox Range Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink, cream or brown, fine to medium-grained, uneven grained to slightly porphyritic leucocratic biotite monzogranite to syenogranite?; commonly miarolitic, granophyric.|
39155|Matchbox Range Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, cream or brown, fine- to medium-grained, seriate to slightly porphyritic biotite monzogranite to syenogranite(?); commonly miarolitic and granophyric; pegmatitic patches. A-type, peraluminous, not peralkaline.|
26728|Maureen Volcanic Group|23291|4|Described|p41, p92 Tb. 3.9|||Formerly included as part of the "Galloway Volcanics". Geological Province: Georgetown Region.||||||19-MAY-15
26728|Maureen Volcanic Group|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
26728|Maureen Volcanic Group|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26728|Maureen Volcanic Group|40860|5|Briefly described|p116|||||||||
26728|Maureen Volcanic Group|43259|6|Mentioned|Appendix 1,p1|||||||||
26728|Maureen Volcanic Group|43740|4|Described|p19|||Maximum thickness about 1500m||||||24-SEP-04
26728|Maureen Volcanic Group|50595|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes: Ironhurst Formation, Puranga Rhyolite.||||||
26728|Maureen Volcanic Group|66529|5|Briefly described|p22-23  |Permian|Late Carboniferous|Minimum age is Early Permian. Age is of a single analysis of a detrital zircon.|<336 +/- 6 Ma (Kositcin, pers. Comm., 2009).||||Includes conglomerate, sandstones, siltstone, volcaniclastic sandstone with rhyolite clasts, muddy sandstone, tuffaceous siltstone and haematitic mudstone.|
26728|Maureen Volcanic Group|67430|5|Briefly described|p60, 62|Early Permian|Late Carboniferous|35km NW of Townsville. Hosts the Maureen U-Mo deposit; syn-mineralisation gangue fluorite shows a mineralisation age of 330 +/- 10 Ma. Appears as Maureen Volcanic Formation on p62.|~340 Ma.|||Correlated with Gilberton Formation.|Basal conglomerate grading upwards through pebbly sandstone, muddy feldspathic sandstone to siltstone. This sequence is overlain by volcaniclastic sandstone with rhyolite clasts, sandstones, tuffaceous siltstone, and hematitic mudstone.|
26728|Maureen Volcanic Group|68352|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Maureen Cauldron. Has reverse remnant magnetisation. Min Age: Early Permian?|||Includes Ironhurst Formation and Puranga Rhyolite.|||19-MAY-15
26728|Maureen Volcanic Group|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
26728|Maureen Volcanic Group|69591|6|Mentioned|p102|Carboniferous|Carboniferous|||||Overlies Gilberton Formation.||
26728|Maureen Volcanic Group|69593|5|Briefly described|p485, p487 |||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|||Ironhurst Formation.||Ignimbrites; minor to locally common sedimentary rocks.|
36128|Mavis Granodiorite|23458|2|Defined|p129, p114|Mesoproterozoic|Mesoproterozoic|Age: 1505+/-7Ma and 1501+/-9Ma. Northern portion of the Capsize granodiorite, now referred to as the Mavis Granodiorite. Intrudes Corella Formation. Medium-grained granodiorite;strongly deformed.  See also p122-123.||||||27-AUG-07
36128|Mavis Granodiorite|23967|6|Mentioned|p1331 Fig.1|||||||||
36128|Mavis Granodiorite|24256|6|Mentioned|p50 Fig.2|||Geological Province: Mount Isa Block.||||||
36128|Mavis Granodiorite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
36128|Mavis Granodiorite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
36128|Mavis Granodiorite|63866|5|Briefly described|p62|Calymmian|Calymmian|Tommy Creek Block.|1505-1500 (Davis et al., 2001)|||||
36128|Mavis Granodiorite|65396|6|Mentioned|p53, p56, p64|Calymmian|Calymmian|Mount Isa Block.|1505 +/- 7 Ma (SHRIMP: Davis et al., 2001)|||||
36128|Mavis Granodiorite|66913|5|Briefly described|p173||||~1500 Ma|||||
36128|Mavis Granodiorite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Canobie Domain, Mount Isa Inlier. Williams Igneous Event. Is presented informally as Mavis granodiorite [?].|1505 +/- 7 Ma.|Williams Supersuite.|||Medium-grained, hornblende-biotite granodiorite; strongly deformed|
36128|Mavis Granodiorite|69056|5|Briefly described|p56-57, Time-Space plot sheet|Calymmian|Calymmian|Another age determination is 1501 +/- 6 Ma (Davis et al., 2001). Has a poorly-defined contact with the Dipvale Granodiorite, which has comparable deformation.|1505 +/- 7 Ma.|Williams Supersuite.|||Strongly deformed, medium-grained hornblende-biotite granodiorite.|
36128|Mavis Granodiorite|69591|5|Briefly described|p59||||1501 +/- 6 Ma (Page and Sun, 1998).|Williams Supersuite.|||Medium-grained, hornblende-biotite granodiorite; strongly deformed.|
36128|Mavis Granodiorite|70532|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium-grained, hornblende-biotite granodiorite; locally strongly deformed.|
36128|Mavis Granodiorite|70574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Medium grained, hornblende biotite granodiorite; locally strongly deformed.|
36128|Mavis Granodiorite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1501+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
36128|Mavis Granodiorite|72596|6|Mentioned|p24|Statherian|Statherian|Geochronologic constraint from Pollard and McNaughton (1997). Now Dipvale Granodiorite, Davis et al. (2001). [Reassigned?]|1752 +/- 8 Ma|||||
36128|Mavis Granodiorite|72799|6|Mentioned|p1, p32, p44|Calymmian|Calymmian|Williams/Naraku Batholiths.|1501 +/- 6 Ma|||||
36128|Mavis Granodiorite|73413|6|Mentioned|App.1|Calymmian|Calymmian|U-Pb SHRIMP igneous crystallisation age of 1501 +/- 6 Ma reported by Pase[Page] and Sun (1998).|1501 +/- 6 Ma|||||
36128|Mavis Granodiorite|73553|4|Described|p2-4, p102-107, p200,|Calymmian|Calymmian|Mary Kathleen Domain, northeast part. Williams-Naraku Igneous Province. Crops out along the SE and western margin of the Dipvale Granodiorite. Outcrops sporadically. Had informally been referred to as Capsize granodiorite. Formally defined by Davis et al., (2001), current distribution is from Withnall et al., (2016). Convoluted and uncertain boundary with Dipvale Granodiorite. Assumed to intrude Dipvale Granodiorite. Yellow to slightly green/blue tones on radiometric images. Descriptions are almost identical to Dipvale Granodiorite. Suggested that only one intrusive unit is present based on lithological, geophysical, structural and geochemical similarity with Dipvale Granodiorite. See also p203-204, p206-208, p210-213.|1505+/-7 Ma, 1501+/-9 Ma zircon U-Pb SHRIMP|Williams Supersuite||Intrudes Corella Formation, intrudes/intercalated with Dipvale Granodiorite|Medium-grained, strongly deformed granodiorite comprising quartz, plagioclase, K-feldspar, hornblende, biotite and magnetite.|03-FEB-23
41265|May Queen Gabbro|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium to coarse-grained, equigranular gabbro, intruded by porphyritic andesite||||||13-DEC-05
41265|May Queen Gabbro|64398|5|Briefly described|Map legend|Early Triassic|Late Permian|Medium- to coarse-grained, equigranular gabbro, intruded by porphyritic andesite.||||||
41265|May Queen Gabbro|65388|4|Described|p326, p301 Fig 98|Late Permian|Late Permian|Mapped in a window in the Jurassic Evergreen Sandstone. Intrudes Carboniferous Rockhampton Group. Probable age given. Dark greenish-grey, medium-grained equigranular to slightly hornblende-phyric gabbro or diorite.||||||
41265|May Queen Gabbro|68679|5|Briefly described|p419|||Occurs as a 1 km2 window in Jurassic sediments south of the Rawbelle Batholith.||||Intrudes Rockhampton Group.|Gabbro.|
76904|Mayfield Gneiss|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event||Wonga Suite, Burstall Suite|||Thinly interlayered to massive, cream to grey, fine to medium grained, strongly foliated, equigranular to locally porphyritic granitic, granodioritic and amphibolitic gneiss; numerous thin felsic sills and veins|
76904|Mayfield Gneiss|69591|5|Briefly described|p60|||Kalkadoon Batholith.|||||Thinly interlayered to massive, cream to grey, fine- to medium-grained, strongly foliated, equigranular to locally porphyritic granitic, granodioritic and amphibolitic gneiss; numerous thin felsic sills and veins.|
76904|Mayfield Gneiss|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Shown as age equivalent to Kalkadoon Granite, Woonigan Granite, Plum Mountain Gneiss.|Thinly interlayered to massive, cream to grey, fine to medium-grained, strongly foliated, equigranular to locally porphyritic granitic, granodioritic and amphibolitic gneiss; numerous thin felsic sills and veins.|
76904|Mayfield Gneiss|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Shown as age equivalent to Kalkadoon Granite, Woonigan Granite, Plum Mountain Gneiss.|Thinly interlayered to massive, cream to grey, fine to medium-grained, strongly foliated, equigranular to locally porphyritic granitic, granodioritic and amphibolitic gneiss; numerous thin felsic sills and veins.|
29973|McBride Basalt Group|23291|3|Fully described|p80 Tb. 3.6, p52|Cenozoic|Cenozoic|Thickness: 500m. Geological Province: McBride Subprovince.||||||30-APR-15
29973|McBride Basalt Group|23502|5|Briefly described|Map Legend||Quaternary|||||||
29973|McBride Basalt Group|23503|5|Briefly described|Map Legend||Pleistocene|||||||
29973|McBride Basalt Group|23616|5|Briefly described|Table 1B p11, p40||Cenozoic|All the rocks in the McBride Basalt Province are assigned to the McBride Basalt Group. McBride Basalt Province.||||||19-NOV-08
29973|McBride Basalt Group|23619|4|Described|p28 table 1|||Also see p13. In the McBride Basalt Province.||||||
29973|McBride Basalt Group|43060|4|Described|p63,Table 1b|Quaternary|Tertiary|late Tertiary to Quaternary age.||||||
29973|McBride Basalt Group|43113|4|Described|p11|||See also Table 1.||||||
29973|McBride Basalt Group|43253|5|Briefly described|map legend|Quaternary|Tertiary|Age late Tertiary to middle Quaternary.||||||
29973|McBride Basalt Group|43716|6|Mentioned|p17|||||||||
29973|McBride Basalt Group|44926|5|Briefly described|Map Legend||Quaternary|||||||
29973|McBride Basalt Group|50201|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
29973|McBride Basalt Group|50202|5|Briefly described|Map legend|Quaternary|Quaternary|Includes: Kinrara Basalt, Murronga Basalt and Mount Joy Basalt. Predominantly olivine basalts.||||||21-MAY-15
29973|McBride Basalt Group|60360|5|Briefly described|Map Legend|Quaternary|Tertiary|Includes: Undara Basalt, Mount Joy Basalt.||||||
29973|McBride Basalt Group|68330|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.|||Includes Depression, Mount Razorback and Undara Basalts.|||
29973|McBride Basalt Group|68331|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.|||Includes Depression, Mount Razorback and Undara Basalts.|||
29973|McBride Basalt Group|68344|5|Briefly described|Map legend.|Quaternary|Tertiary||||Includes Mount Joy, Murronga and Kinrara Basalts.||Olivine basalt: flows, vents or plugs.|
29973|McBride Basalt Group|68346|5|Briefly described|Map legend.|Quaternary|Tertiary|Of McBride Basalt Province.|||Includes Mount Joy Basalt.||Olivine basalt.|
29973|McBride Basalt Group|68405|5|Briefly described|Map Legend|Quaternary|Paleogene|Tertiary maximum age.|||Includes Undara Basalt and two unnamed basalts.||Olivine basalt.|
29973|McBride Basalt Group|68477|5|Briefly described|Map Legend|Pleistocene|Neogene|McBride Basalt Province.|||Includes Undara Basalt and Mount Joy Basalt.||Olivine Basalt.|24-SEP-14
29973|McBride Basalt Group|68480|5|Briefly described|Map Legend|Quaternary|Neogene |McBride Basalt Province. Late Tertiary - Quaternary (Neogene) age.|||||Olivine basalt.|
29973|McBride Basalt Group|68481|5|Briefly described|Map Legend|Neogene |Neogene |McBride Basalt Province. Late Tertiary - Quaternary (Neogene) age.|||||Olivine basalt.|
29973|McBride Basalt Group|68553|6|Mentioned|Map legend|Quaternary|Neogene|Parts of both this unit and the Nulla Basalt Group; the Atherton, Chudleigh, McIvor River, McLean, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn. Parts of this unit, as well as the Barkers and Yates Creek Basalts; the Maer Volcanics; parts of the Nulla Basalt Group, and unnamed basalt flows, are all mapped under the symbol, Qbn.||||||
29973|McBride Basalt Group|69599|5|Briefly described|p642|Quaternary|Pliocene|McBride Province. Comprises 10 Quaternary units and older, unnamed Pliocene or Pleistocene flows. Geochemistry briefly described. Lava tubes and long lava flows are a feature of the Province.|<2.7 Ma to <50 ka.||||Predominantly mafic: nephelinite and basanite, hawaiite and minor mugearite and phonolite. Compositionally diverse mantle and lower-crust xenoliths locally abundant.|
29973|McBride Basalt Group|69789|5|Briefly described|p1041|Pleistocene|Pliocene|Flood basalt fields and related volcanic centres. Extensively developed in NE Queensland.|<5 Ma (Stephenson et al., 1980).|||||
29973|McBride Basalt Group|73115|6|Mentioned|[See comments]|||McBride Basalt Province. Contains distinct basalts with intervening palaeosols. Aquifers hosted in fractured, weathered, and vesicular zones. Associated with persistent wet areas / springs. Contributes the first reliable [groundwater] input to the Burdekin River. p: 25, 28-31, 39, 43, 48, 53, 58-59, 63, 65, 68, 132.||||||
26021|McDermott Formation|22538|6|Mentioned|Fig3 P709|||||||||
26021|McDermott Formation|22670|6|Mentioned|55|||Geol. province: McArthur Basin.||||||06-NOV-06
26021|McDermott Formation|23065|5|Briefly described|16|Proterozoic|Proterozoic|Of Tawallah Group.||||||29-FEB-08
26021|McDermott Formation|23395|5|Briefly described|p388|||||||||
26021|McDermott Formation|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||06-NOV-06
26021|McDermott Formation|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26021|McDermott Formation|23867|5|Briefly described|p16|||Formerly the "Aquarium Formation" (in part?).  Of Tawallah Group.  Correlates with Cottee Formation (Katherine River Group).  Geological Province: McArthur Basin.  See also Fig. 30.||||||29-FEB-08
26021|McDermott Formation|24050|5|Briefly described|p19|||Of the Tawallah Group.||||||06-NOV-06
26021|McDermott Formation|31421|6|Mentioned|p507|||||||||
26021|McDermott Formation|32660|5|Briefly described|Table 4|||||||||
26021|McDermott Formation|33665|6|Mentioned|p365|||See also p368.||||||06-NOV-06
26021|McDermott Formation|35114|6|Mentioned|p203|||||||||
26021|McDermott Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|36012|3|Fully described|Table 2|||||||||
26021|McDermott Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|37568|5|Briefly described|p78|||||||||
26021|McDermott Formation|38582|6|Mentioned|Fig.3|||||||||
26021|McDermott Formation|38584|4|Described|p14|||||||||
26021|McDermott Formation|39445|5|Briefly described|Table 2|||See also p36.||||||06-NOV-06
26021|McDermott Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|40489|6|Mentioned|p89|||||||||
26021|McDermott Formation|40691|5|Briefly described|p9|||||||||
26021|McDermott Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|41721|3|Fully described|p18|||Of the Tawallah Group. Conformably overlies Seigal Volcanics. Thickness: 200m. Geological province: McArthur Basin. Dolomite, siltstone and sandstone.||||||01-AUG-07
26021|McDermott Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26021|McDermott Formation|42385|6|Mentioned|Fig.5 P8|||||||||
26021|McDermott Formation|42812|5|Briefly described|p14|||see also Fig.5||||||
26021|McDermott Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||06-NOV-06
26021|McDermott Formation|43036|6|Mentioned|Fig.5|||||||||
26021|McDermott Formation|44287|14|Not recorded|p.8|||(E53-3).||||||
26021|McDermott Formation|44305|14|Not recorded|p.11-12||Neoproterozoic|(E53-8). opp.6,18. U.Prot.||||||
26021|McDermott Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26021|McDermott Formation|44473|14|Not recorded|p.8, opp. p.7|||(E53-7). L?Prot.||||||
26021|McDermott Formation|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26021|McDermott Formation|45162|2|Defined|p14|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|45166|5|Briefly described|p28|||||||||
26021|McDermott Formation|46804|6|Mentioned|p154|||||||||
26021|McDermott Formation|49001|6|Mentioned|p5|||||||||
26021|McDermott Formation|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
26021|McDermott Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Sly Creek Sandstone, underlain by Seigal Volcanics.||||||
26021|McDermott Formation|63112|5|Briefly described|p1191 Fig.2, p1192, p1205|||Leichhardt Superbasin. Age approximated from Fig.2. 120-500 m thick.|c.1755-1757 Ma.||||Interbedded dolostone, chert, halite-cast-bearing mudstone, glauconitic sandstone, stromatolitic dolostone, and shales.|
26021|McDermott Formation|63866|5|Briefly described|p54, p56|||||||Equivalent to the Quilalar Supersequence.||
26021|McDermott Formation|64817|6|Mentioned|p353 Fig.4,p355 Fig.5,p367 Tb.2,p369  |||||Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
26021|McDermott Formation|65228|5|Briefly described|p21, Figs.02, 06, 07.|||McArthur Basin. Carbonate unit; map symbol Ptd.||Unit in Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Wununmantyala Sandstone. Is equivalent to Sly Creek Sandstone.||
26021|McDermott Formation|65340|4|Described|p12 Fig.6, pp92-93. |||Revised in this study to include areas mapped as Aquarium Formation by Pietsch et al. (1991a) and Haines et al. (1993) in the Batten Fault Zone. Also now includes sedimentary intervals in BAUHINIA DOWNS and MOUNT YOUNG maps that had been assigned to the Settlement Creek Dolerite.||Unit in Tawallah Group.||Overlies Sly Creek Sandstone. Is disconformably overlain by Wununmantyala Sandstone.|Sandstone, dolostone and mudstone.|
26021|McDermott Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Sly Creek Sandstone.|Fine- to medium-grained quartz, glauconitic and dolomitic sandstone; dolostone, siltstone and chert interbeds.|
26021|McDermott Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p32|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin.|~1750-1740 Ma.|Tawallah Group|||Stromatolitic and oolitic dolomite, sandstone, shale and siltstone.|
26021|McDermott Formation|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. Over 400m thick.||Tawallah Group||Overlies (conformably) Seigal Volcanics. Is conformably overlain by Sly Creek Sandstone.|Fine- to medium-grained quartz, glauconitic and dolomitic sandstone, dolostone, siltstone and chert interbeds.|
26021|McDermott Formation|69430|4|Described|p15:3, 10-12|||Jackson et al. (1987). Includes outcrops previously part of the Aquarium Formation in the Batten Fault Zone and SW McArthur Basin. 200m thick. Shallow-water marginal marine deposits: subtidal to supratidal carbonate bank shoreline facies. Is said to be overlain by Sly Creek Sandstone: this contradicts the relationships shown in Fig.15.4, and is inconsistent with Sly Creek Sandstone being correlated with upper Seigal Volcanics which conformably underlies McDermott Formation.||Tawallah Group.||Conformably overlies Seigal Volcanics. Is overlain conformably by Wununmantyala Sandstone.|Alternating bands of shallow-marine dolostone and siltstone, with sandstone at the base.|12-JUL-16
26021|McDermott Formation|69591|5|Briefly described|p39, p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|Dolomite, sandstone, siltstone.|
26021|McDermott Formation|69673|4|Described|p16 fig 13, p24, p32, p33, p40|||Mixed carbonates and clastic sedimentary rock. Deposited in shallow marine, subtidal to supratidal settings. Possible source rock.||Tawallah Group||Disconformably overlain by Wununmantyala Sandstone, Conformably overlies Rosie Creek Sandstone Member|Dolostone, chert, mudstone and sandstone.|
26021|McDermott Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Sly Creek Sandstone.|Dolomite, laminated, stromatolitic, sandy, oolitic and interclast-rich; dolarenite; quartz sandstone with interbedded shale; glauconitic sandstone; shale and siltstone.|
26021|McDermott Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Tawallah Group.||||
26021|McDermott Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group||Overlies Rosie Creek Sandstone Member and underlies Wununmantyala Sandstone.||
26021|McDermott Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group|Rosie Creek Sandsotne Member?|Underlain by Rosie Creek Sandstone Member. Overlain by Wununmantyala Sandstone.||
26021|McDermott Formation|72912|4|Described|p5 Fig.3, p17, p19, p31 Fig.11, p36.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Hydrocarbon shows known and TOC is discussed.||Tawallah Group||Overlies Rosie Creek Sandstone Member and underlies Wununmantyala Sandstone.||15-MAR-21
26021|McDermott Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.||Tawallah Group||Underlain by Rosie Creek Sandstone Member. Overlain by Wununmantyala Sandstone.||
26021|McDermott Formation|73412|5|Briefly described|p4, 8-9|||Southern McArthur Basin. Non-magnetic.||Tawallah Group.||Overlies Rosie Creek Sandstone. Is overlain unconformably by Wununmantyala Sandstone.||
30332|McDougall Creek rhyolite|43259|4|Described|Appendix 1,p4|||May be related to Rokehurst Creek rhyolite. Carboniferous?||||||
27647|McFarlanes Andesite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Mount Little Volcanic Group. Age: >/=275Ma. Geological Province: Georgetown Region.||||||04-JUN-15
27647|McFarlanes Andesite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V3.||||||
27647|McFarlanes Andesite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
27647|McFarlanes Andesite|40659|6|Mentioned|p250|||||||||
27647|McFarlanes Andesite|40860|4|Described|p110|||||||||
27647|McFarlanes Andesite|40954|6|Mentioned|p133|||||||||
27647|McFarlanes Andesite|43259|4|Described|Appendix 1,p1.||Permian|Age 275+/-1 Ma.||||||
27647|McFarlanes Andesite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.||Conformably overlies Little Pocket Dacite.|Amygdaloidal two-pyroxene andesite, generally agate-bearing.|
27647|McFarlanes Andesite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Mount Little Volcanic Group.||Conformably overlies Little Pocket Dacite.|Amygdaloidal two-pyroxene andesite, generally agate-bearing.|
22290|McIlwraith Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Coen Metamorphics.||||||
22290|McIlwraith Granite|43741|3|Fully described|p9|Devonian|Silurian|Age: approx 407 Ma. 'informal unit'||||||
22290|McIlwraith Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
22290|McIlwraith Granite|71792|5|Briefly described|p25-p26|||||||Faulted against the Buthen Buthen Granite (interpreted).||
22290|McIlwraith Granite|71849|3|Fully described|p2, p5-6, p8, p14, p18, p50, p70-81|Devonian|Devonian|See also p104, p130, p147, p150, p155-157, p173, p184, p195. Previously depicted as part of the Kintore Adamellite. Informally referred to as McIlwraith granite by Knutson et al. (1994). Forms McIlwraith Range after which it is named, a N-trending belt ~70km long and up to ~15km wide, NE of Coen. Proposed type area is around MGA 760622 8520171. Geophysics described. Lithologies described in great detail; photomicrographs. Cut by numerous dykes (described). Not isotopically dated; has mineralogical and geochemical similarities to Ebagoola Suite units.||Ebagoola Suite.||Intrudes the Coen and Newberry Metamorphic Groups, and Leo Creek Granodiorite (inferred). Is intruded by Twin Humps Granite. Is overlain nonconformably by Falloch and Lilyvale beds.|Mainly high-K calc-alkaline S-type. Several rock types, including two-mica monzogranites and granodiorite-tonalite. Minor to trace garnet, rare sillimanite and altered cordierite.|
22290|McIlwraith Granite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Grey, medium, seriate porphyritic biotite-muscovite monzogranite; pale grey, fine-medium slightly porphyritic biotite granodiorite-tonalite; moderately porphyritic muscovite-biotite leucogranite; cordierite-sillimanite-garnet-muscovite monzogranite.|
22290|McIlwraith Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Grey medium seriate, porphyritic biotite-muscovite monzogranite; pale grey, fine-medium, slightly porphyritic biotite granodiorite/tonalite; moderately porphyritic, muscovite-biotite leucogranite; cordierite-sillimanite-garnet-muscovite monzogranite.|
23778|McIvor River Basalt|23423|5|Briefly described|p261|||McIvor Subprovince.||||||
23778|McIvor River Basalt|23511|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
23778|McIvor River Basalt|23512|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
23778|McIvor River Basalt|42369|5|Briefly described|p64, Fig.3 p18|||Formerly part of Piebald Basalt Province. Reserved 1990.||||||01-JUN-09
23778|McIvor River Basalt|44872|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
23778|McIvor River Basalt|50587|5|Briefly described|Map Legend|Pleistocene|Pliocene|Nephelinite, basanite, hawaiite and mugearite; minor scoria, lapilli tuff.||||||28-JUN-04
23778|McIvor River Basalt|60425|4|Described|p42 Tb. 3, p110|Pleistocene|Pliocene|Age is Pliocene?- Pleistocene. Thickness: ~30m? Unconformably overlies Hodgkinson Formation. Basanite, hawaiite, mugearite, nephelinite; minor scoria, lapilli tuff.||||||07-FEB-11
23778|McIvor River Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, Chudleigh, McLean, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
23778|McIvor River Basalt|69599|5|Briefly described|p642|||McIvor Province, in the Morgan-McIvor valley.|1.6-1.2 Ma (Stephenson, 1989).||||Basanite, hawaiite, mugearite and minor olivine tholeiite. Valley-fill lava flows and very minor pyroclastic deposits.|
27484|McKinnons Creek Granite|23032|5|Briefly described|p37,38|||||||||
27484|McKinnons Creek Granite|23291|4|Described|p89 Fig. 3.8|||Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27484|McKinnons Creek Granite|23430|5|Briefly described|p486|||||||||
27484|McKinnons Creek Granite|23453|5|Briefly described|p22|Early Devonian|Early Devonian|||||||
27484|McKinnons Creek Granite|23494|5|Briefly described|p10, p23 Tb. 1|Precambrian|Precambrian|Coarse, even-grained cream-pink muscovite granite.  Intrudes Sandalwood Serpentinite and Lucky Creek Formation.||||||
27484|McKinnons Creek Granite|23498|5|Briefly described|p24 table1||Proterozoic|Intrudes Paddys Creek Formation and Lucky Creek Formation. Unconformably overlain by Crooked Creek Conglomerate Member||||||
27484|McKinnons Creek Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 61. Assumed to be I-Type.||||||
27484|McKinnons Creek Granite|23619|4|Described|p41 Table 2|Early Devonian|Silurian|Intrudes Einasleigh Metamorphics and Dido Tonalite. Also see p7. Georgetown Province.||||||
27484|McKinnons Creek Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27484|McKinnons Creek Granite|31832|6|Mentioned|Table 6|||||||||
27484|McKinnons Creek Granite|32528|5|Briefly described|Table 1|||||||||
27484|McKinnons Creek Granite|32553|4|Described|p62|||||||||
27484|McKinnons Creek Granite|37614|4|Described|p237|||See also P233.||||||
27484|McKinnons Creek Granite|37768|5|Briefly described|p42|||||||||
27484|McKinnons Creek Granite|39027|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
27484|McKinnons Creek Granite|39445|5|Briefly described|Table 2|||See also P45||||||
27484|McKinnons Creek Granite|39689|6|Mentioned|Fig.2|||||||||
27484|McKinnons Creek Granite|39981|6|Mentioned|p102|||||||||
27484|McKinnons Creek Granite|40746|5|Briefly described|p358|||||||||
27484|McKinnons Creek Granite|41675|1|Redefined|p63|Late Silurian?||Or Early Devonian?||||||
27484|McKinnons Creek Granite|41680|6|Mentioned|p117|||||||||
27484|McKinnons Creek Granite|42054|6|Mentioned|p273|||||||||
27484|McKinnons Creek Granite|42279|6|Mentioned|Fig.2 P18|||||||||
27484|McKinnons Creek Granite|42933|6|Mentioned|p221|||||||||
27484|McKinnons Creek Granite|43113|4|Described|Table 2 p26|Early Devonian|Silurian|||||||
27484|McKinnons Creek Granite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
27484|McKinnons Creek Granite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
27484|McKinnons Creek Granite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||08-MAY-15
27484|McKinnons Creek Granite|44043|14|Not recorded|Tb.1,Fig.8||Late Precambrian|Intrudes Halls Reward Metamorphics,Stenhouse Creek Amphibolite, Lucky Creek Formation, Paddys Creek Formation and Sandalwood Serpentinite.||||||
27484|McKinnons Creek Granite|44048|14|Not recorded|Map Legend||Proterozoic|||||||
27484|McKinnons Creek Granite|44049|14|Not recorded|Map Legend||Proterozoic|||||||
27484|McKinnons Creek Granite|44059|2|Defined|p442,445-447|||Proterozoic or Early Palaeozoic.||||||
27484|McKinnons Creek Granite|44515|14|Not recorded|p35|||No age given.||||||
27484|McKinnons Creek Granite|45009|2|Defined|p21,28,75,79,101-4,|||Pl.13,Tb.2. Unconformably overlain by Crooked Creek Conglomerate.||||||18-DEC-13
27484|McKinnons Creek Granite|50200|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
27484|McKinnons Creek Granite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
27484|McKinnons Creek Granite|50202|5|Briefly described|Map legend|Late Silurian|Late Silurian|Biotite-muscovite granite and muscovite-biotite granite.||||||
27484|McKinnons Creek Granite|67455|6|Mentioned|p575 Table 1. |Silurian|Silurian|Greenvale Province.|||||Weakly foliated granitoid.|
27484|McKinnons Creek Granite|68336|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith.|||||Cream, foliated garnet-muscovite, biotite-muscovite and muscovite-biotite granite.|
27484|McKinnons Creek Granite|68341|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith.|||||Cream, foliated garnet-muscovite, biotite-muscovite and muscovite-biotite granite.|
27484|McKinnons Creek Granite|68344|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Cream, foliated biotite-muscovite to muscovite-biotite granite.|
27484|McKinnons Creek Granite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Weakly to non-magnetic.|||||Cream, foliated, biotite-muscovite to muscovite-biotite granite.|
27484|McKinnons Creek Granite|68410|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Dido Batholith.|||||Cream, locally foliated biotite-muscovite to muscovite-biotite granite; cream biotite-muscovite granite.|
27484|McKinnons Creek Granite|68576|6|Mentioned|Q_11: p31-32|Silurian|Silurian|Very poorly exposed.||||||
27484|McKinnons Creek Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
26022|McLean Basalt|23423|4|Described|p261||Cenozoic|Two periods of volcanic activity: 6.29 Ma-5.12 Ma and 3.6-3.08 Ma. McLean Subprovince.||||||19-NOV-08
26022|McLean Basalt|23511|5|Briefly described|Map Legend||Tertiary|||||||
26022|McLean Basalt|24086|5|Briefly described|p315 Fig. 2|Tertiary|Tertiary|Geological Province: Hodgkinson Basin.||||||
26022|McLean Basalt|24213|5|Briefly described|p778 Fig. 2|Tertiary|Tertiary|||||||
26022|McLean Basalt|31832|6|Mentioned|Table 6|||||||||
26022|McLean Basalt|34046|6|Mentioned|Table III|||||||||
26022|McLean Basalt|37607|6|Mentioned|Fig.6|||||||||
26022|McLean Basalt|39445|5|Briefly described|Table 14|||||||||
26022|McLean Basalt|42304|2|Defined|p33|Quaternary|Tertiary|Age range: 4Ma to 0.5Ma||||||22-APR-09
26022|McLean Basalt|42632|3|Fully described|p2-25|||||||||
26022|McLean Basalt|43098|4|Described|p49|Late Miocene|Late Eocene|||||||
26022|McLean Basalt|43285|5|Briefly described|Map Legend||Tertiary|||||||
26022|McLean Basalt|43625|4|Described|p48||Tertiary|Age: 3.1-6.3 Ma||||||
26022|McLean Basalt|43896|14|Not recorded|Map Legend|Quaternary|Tertiary|||||||
26022|McLean Basalt|43979|4|Described|p65,67-69,70||Cenozoic|||||||19-NOV-08
26022|McLean Basalt|44292|14|Not recorded|Tb.1,opp.p8|||Correlated with Piebald Basalt.||||||
26022|McLean Basalt|44293|14|Not recorded|Map Legend||Tertiary|||||||
26022|McLean Basalt|44294|2|Defined|Tb.2,p8,9,15-17,26||Tertiary|Map. Overlies Hodgkinson Formation and Dalrymple Sandstone.||||||
26022|McLean Basalt|45025|4|Described|p113-114|Quaternary|Tertiary|||||||
26022|McLean Basalt|45087|5|Briefly described|p165|||Chem. analyses. See also P198.||||||
26022|McLean Basalt|50335|5|Briefly described|Map Legend|Pleistocene|Miocene|Porphyritic olivine basalt lava; commonly amygdaloidal or vesicular.||||||21-JUN-04
26022|McLean Basalt|50596|5|Briefly described|Map Legend|Quaternary|Tertiary|Pyroclastic deposits, basalt lava flows.||||||
26022|McLean Basalt|50630|5|Briefly described|Map Legend|Pleistocene|Miocene|Nephelinite and olivene basalt.||||||
26022|McLean Basalt|60358|5|Briefly described|Map Legend|Pleistocene|Miocene|Basic lava, minor pyroclastic deposits.||||||
26022|McLean Basalt|60425|3|Fully described|p42-43 Tb. 3|Quaternary|Miocene|Unconformable on/faulted against Hodgkinson Fm; unconformably overlies Normanby Formation. Age: ~9Ma-0.5Ma (K-Ar). Detailed lithology presented.||||||07-FEB-11
26022|McLean Basalt|61155|5|Briefly described|p20|Pleistocene|Late Pliocene|In eastern Cape York.||||||
26022|McLean Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, Chudleigh, McIvor River, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
26022|McLean Basalt|70673|6|Mentioned|p100|Quaternary|Tertiary|Lakeland Downs-Maytown region.||||||
23780|McLennons Creek Rhyolite|23032|5|Briefly described|p43||Carboniferous|||||||
23780|McLennons Creek Rhyolite|23291|4|Described|p91 Fig. 3.9|Carboniferous|Carboniferous|Parent: Butlers Volcanic Group. Age: About 330Ma. Thickness: 150-300+m. Geological Province: Georgetown Region.||||||08-JUL-15
23780|McLennons Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V33. I-Type.||||||
23780|McLennons Creek Rhyolite|23619|4|Described|p32 Table 1||Carboniferous|Butlers Volcanic Group. Underlying units Einasleigh Metamorphics and Oak River Granodiorite - unconformable. Also Edmonds Creek Rhyolite.||||||
23780|McLennons Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23780|McLennons Creek Rhyolite|40542|6|Mentioned|p97|||||||||
23780|McLennons Creek Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Butlers Volcanic Group.||||||
23780|McLennons Creek Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Butlers Volcanic Group||||||
23780|McLennons Creek Rhyolite|43259|4|Described|Appendix 1,p4.||Carboniferous|of Butlers Volcanic Group.||||||
23780|McLennons Creek Rhyolite|43286|5|Briefly described|Map Legend||Carboniferous|of Butlers Volcanic Group.||||||
23780|McLennons Creek Rhyolite|43740|4|Described|p24|||||||||
23780|McLennons Creek Rhyolite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Butlers Volcanic Group.||||||
23780|McLennons Creek Rhyolite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of the Butlers Volcanic Group.||||||
23780|McLennons Creek Rhyolite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|High K, Th and U radiometric responses.||Unit in Butlers Volcanic Group.||Conformably overlies Edmonds Creek Rhyolite.|Brown, crystal-poor to moderately crystal-rich rhyolitic ignimbrite.|
23780|McLennons Creek Rhyolite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure.||Of the Butlers Volcanic Group.||Conformably underlain by the Edmonds  Creek Rhyolite.|Brown, crystal-poor to moderately crystal-rich rhyolitic ignimbrite.|
68958|McLeod Granite|60425|4|Described|p80, p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla S'suite). Fine-grained, highly porphyritic (clinopyroxene-) garnet-biotite-orthopyroxene granite - accessory ilmenite, zircon, apatite, apatite, sillimanite, muscovite - detailed lith (p275).||||||07-FEB-11
68958|McLeod Granite|69593|5|Briefly described|p479, p482|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Curraghmore Suite.|||S-type; contains microdioritic enclaves that may represent autoliths.|
67841|McNamara Group, Lower|24432|6|Mentioned|p565 Fig.4|||||||||
67841|McNamara Group, Lower|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mount Isa Inlier.|~1690-1650 Ma.||Torpedo Creek, Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta Formations.|||
67841|McNamara Group, Lower|68542|5|Briefly described|p6, p8||||||Includes Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation|Overlies Surprise Creek beds, overlain by Upper McNamara Group|Marine carbonates and clastic sedimentary rocks.|22-OCT-19
67841|McNamara Group, Lower|68576|4|Described|Q_2: p6, p8|Proterozoic|Proterozoic|Lawn Hill Platform, Mount Isa Inlier. Hosts the exceptionally high-grade, sediment-hosted Lady Loretta Pb-Zn deposit, and the Lady Annie (Cu) Project (both described in detail).|||Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation.|Overlies Surprise Creek Beds. Is overlain by Upper McNamara Group.|Basal coarse clastics fining upwards into a thick sequence of dolomitic siltstones and sandstones. Occasional local non-dolomitic quartz-clastic sediments. Chert horizons common.|
67841|McNamara Group, Lower|73083|6|Mentioned|p54|||||||||
40828|McNamara Group, Upper|23957|6|Mentioned|p1124|||Informal - refers to McNamara Group.||||||16-DEC-04
40828|McNamara Group, Upper|24432|6|Mentioned|p565 Fig.4|||||||||
40828|McNamara Group, Upper|50550|5|Briefly described|p1146 Fig.9, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
40828|McNamara Group, Upper|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mount Isa Inlier.|~1650-1590 Ma.||Shady Bore Quartzite, Riversleigh Siltstone, Termite Range and Lawn Hill Formations.|||
40828|McNamara Group, Upper|68542|6|Mentioned|p6||||||Includes Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation.|Overlies Lower McNamara Group, overlain by South Nicholson Group.||
40828|McNamara Group, Upper|68576|4|Described|Q_2: p6|Proterozoic|Proterozoic|Lawn Hill Platform, Mount Isa Inlier.|||Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation.|Overlies Lower McNamara Group. Is overlain unconformably by South Nicholson Group.|Non-dolomitic clastic facies associated with deeper water conditions, sometimes as turbidites.|
40828|McNamara Group, Upper|73083|6|Mentioned|p54, p69|||||||||
23782|Meadowvale Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
23782|Meadowvale Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23782|Meadowvale Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 85. I-Type.||||||
23782|Meadowvale Granodiorite|42245|2|Defined|p39|Early Devonian|Late Silurian|||||||
23782|Meadowvale Granodiorite|42750|6|Mentioned|p36, p46|||||||||
23782|Meadowvale Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23782|Meadowvale Granodiorite|43259|4|Described|Appendix 1,p21.|Early Devonian|Late Silurian|Late Silurian - Early Devonian? Probably related to Casey Spring Creek & Five Mile Mill Granodorites||||||
23782|Meadowvale Granodiorite|43933|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23782|Meadowvale Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23782|Meadowvale Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Meadowvale gdrt.||Unit in Millchester Supersuite.||||
23782|Meadowvale Granodiorite|71031|5|Briefly described|p57|Silurian|Silurian|||Millchester Supersuite||Overlain by the Fanning River Group.||
24376|Meath Rhyolite Member|23032|4|Described|p37|Visean|Visean|||||||
24376|Meath Rhyolite Member|23422|5|Briefly described|p181|||Of Lyall Formation.||||||
24376|Meath Rhyolite Member|23424|5|Briefly described|Table 8.1 Fig 8.4||Visean|Of Lyall Formation/Clarke River Group, Clarke River Basin.||||||
24376|Meath Rhyolite Member|23430|5|Briefly described|p508|||Lyall Formation. Clarke River Basin.||||||
24376|Meath Rhyolite Member|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic Member No. V45. Assumed to be I-Type.||||||
24376|Meath Rhyolite Member|23893|5|Briefly described|p18|||Of Lyall Formation.  Geological Province: Clarke River Basin.||||||
24376|Meath Rhyolite Member|40943|2|Defined|p56|Late Carboniferous|late Visean|Late Visean to Late Carboniferous||||||
24376|Meath Rhyolite Member|41260|5|Briefly described|p23|||||||||
24376|Meath Rhyolite Member|41735|6|Mentioned|p286|||||||||
24376|Meath Rhyolite Member|41776|6|Mentioned|p527|||||||||
24376|Meath Rhyolite Member|41823|5|Briefly described|p159|||||||||
24376|Meath Rhyolite Member|41824|6|Mentioned|p201|||||||||
24376|Meath Rhyolite Member|41916|6|Mentioned|p33|||||||||
24376|Meath Rhyolite Member|42692|5|Briefly described|map legend|Early Carboniferous|Late Devonian|||||||
24376|Meath Rhyolite Member|42933|4|Described|p212|||of Lyall Formation||||||
24376|Meath Rhyolite Member|43095|6|Mentioned|p65|||of Lyall Formation||||||
24376|Meath Rhyolite Member|43259|4|Described|Appendix 1,p5.||Early Carboniferous|of Clarke River Group. Age Early Carboniferous?Part of Lyall Formation.||||||21-JUN-13
24376|Meath Rhyolite Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Lyall Formation.||||||
24376|Meath Rhyolite Member|60705|5|Briefly described|p649|||Welded rhyolite ignimbrites. Geological Province: Clarke River Basin.||||||12-APR-05
24376|Meath Rhyolite Member|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Lyall Formation.|||Pink to brown, crystal-rich rhyolitic ignimbrite; minor volcanolithic sandstone and conglomerate.|
24376|Meath Rhyolite Member|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin. High K, Th and U radiometric responses.||Unit in Lyall Formation.|||Pink to brown, crystal-rich rhyolitic ignimbrite; minor volcanilithic sandstone and conglomerate.|
24376|Meath Rhyolite Member|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin. High K, Th and U radiometric responses.||Unit in Lyall Formation.|||Pink to brown, crystal-rich rhyolitic ignimbrite; minor volcanilithic sandstone and conglomerate.|
24376|Meath Rhyolite Member|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Lyall Formation.|||Pink to brown, crystal-rich rhyolitic ignimbrite; minor volcanolithic sandstone and conglomerate.|
24376|Meath Rhyolite Member|68478|5|Briefly described|Map Legend|||Equivalents of this unit may occur within the Lyall Formation of the Clarke River Group.||||||
24376|Meath Rhyolite Member|68479|5|Briefly described|Map Legend|||Equivalents of this unit may occur in the Lyall Formation of the Clarke River Group.||||||
24376|Meath Rhyolite Member|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province.||Lyall Formation.||||
24376|Meath Rhyolite Member|69592|5|Briefly described|p275-276|Visean|Visean|Clarke River Basin. Up to 40m thick.||Lyall Formation.|||An interval near the middle of the Formation, comprising ignimbrite interlayered with sandstone.|
24376|Meath Rhyolite Member|69593|5|Briefly described|p495|Carboniferous|Carboniferous|Charters Towers region; Broken River Province.||Lyall Formation.||||
30162|Medial Formation|43100|6|Mentioned|p40|||||||||
30104|Medicine Creek Complex|22847|3|Fully described|p 9, 38|||||||||
30104|Medicine Creek Complex|23504|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
30104|Medicine Creek Complex|23513|5|Briefly described|Map legend||Early Ordovician|Palaeozoic Intrusive No. 495. I-Type.||||||
30104|Medicine Creek Complex|43093|4|Described|Appendex 1|||Variation on Medicine Creek Granodiorite?[CEBMar96]||||||
30104|Medicine Creek Complex|43259|4|Described|Appendix 1,p51.|Early Ordovician|Cambrian|||||||
30104|Medicine Creek Complex|43936|5|Briefly described|Map Legend|Devonian|Neoproterozoic|||||||
38212|Medicine Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Cambrian|||||||
38212|Medicine Supersuite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
80678|Meldrum Granite|71849|3|Fully described|p4, p8, p17, p33, p46-50, p149, p162-168|Devonian|Devonian|See also p195. New name. Previously a minor constituent of the Morris Adamellite of Trail et al. (1969), Willmott et al. (1973) and Whitaker and Gibson (1977). Ovoid, elongate pluton ~15km long and up to ~5km wide, c.25-30km NNW of Coen airport. Crops out as scattered large boulders and tors, and pavements in watercourses. The type area is around MGA 714731 8503812. Named after the Parish of Meldrum, in which the northern half of the pluton crops out. Shares many characteristics with Morris Granite. Has geochemical similarities to A-type granites. Not yet isotopically dated. A member of the Pama Igneous Association.||Blue Mountains Supersuite.||Intrudes Yarraden Schist. Is overlain nonconformably by Gilbert River Formation and Falloch beds.|White to pale grey, medium-grained, highly porphyritic (tourmaline-allanite-titanite-hornblende-)biotite monzogranite containing numerous coarse K-feldspar phenocrysts. I-type.|
80678|Meldrum Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Blue Mountains Supersuite.|||Pale grey, medium- to coarse-grained, slightly to highly and coarsely porphyritic (garnet-)biotite-muscovite granite; irregularly distributed K-feldspar megacrysts to ~15cm; extensively deformed and recrystallised.|
30148|Melody Rocks Limestone|43098|5|Briefly described|p20|||||||||
26026|Melon Creek Tonalite|23422|5|Briefly described|p173, p210 Table 6.6|Middle Ordovician|Middle Ordovician|Probably part of the Columbia Creek Supersuite.||||||
26026|Melon Creek Tonalite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
26026|Melon Creek Tonalite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 174. ?S-Type.||||||
26026|Melon Creek Tonalite|42407|2|Defined|p38|Early Devonian|Ordovician|Reserved as Melon Creek Granodiorite.||||||
26026|Melon Creek Tonalite|42474|5|Briefly described|p28|||||||||
26026|Melon Creek Tonalite|42689|5|Briefly described|map legend|Early Paleozoic||||||||07-NOV-08
26026|Melon Creek Tonalite|43095|5|Briefly described|Plate 1|||||||||
26026|Melon Creek Tonalite|43259|4|Described|Appendix 1,p27.|Devonian|Ordovician|Ordovician to Devonian?.||||||
26026|Melon Creek Tonalite|43589|6|Mentioned|p18|Paleoproterozoic|Paleoproterozoic|Taralee Volcanics faulted against this unit.||||||07-NOV-08
26026|Melon Creek Tonalite|68419|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained biotite tonalite.|
26026|Melon Creek Tonalite|68420|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, medium-grained biotite tonalite.|
37120|Melrose Igneous Complex|23799|3|Fully described|p75|Triassic|Permian|Previously included with Boondooma Igneous Complex (Murphy et al, 1976).  Intrudes the Fifer Creek Metamorphics.  Of the South-east Queensland Volcanic and Plutonic Province. See also p13 Tb. 1||||||
37120|Melrose Igneous Complex|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
37120|Melrose Igneous Complex|60371|5|Briefly described|Map Legend|Triassic|Permian|Biotite (-hornblende) granite and granodiorite; diorite and quartz microdiorite.||||||02-SEP-04
37120|Melrose Igneous Complex|68679|6|Mentioned|p323|||Proximity to this unit (and other named units) increases the metamorphic grade of rocks in the Fifer Creek Metamorphics.||||||
36452|Melville Supersuite|23430|6|Mentioned|495p|||I-Type granites.||||||
33428|Memerambi Granite|23799|3|Fully described|p98, p11 Tb. 1|Triassic|Triassic|Previously mapped as part of the Boondooma Igneous Complex (Murphy et al, 1976).  Overlain by Tarong beds and Main Range Volcanics, unconformably.  Of the South-east Queensland Volcanic and Plutonic Province.||||||
33428|Memerambi Granite|23800|5|Briefly described|Map Legend|Triassic|Triassic|||||||
33428|Memerambi Granite|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||11-JUN-04
33428|Memerambi Granite|60371|5|Briefly described|Map Legend|Triassic|Triassic|Hornblende-biotite granite.||||||
33428|Memerambi Granite|68679|5|Briefly described|p413, p415|Early Triassic|Permian|West of the Esk Basin, northern New England Orogen. Originally part of the Boondooma Igneous Complex (Murphy et al., 1976). Has multiple plutons with highly magnetic margins.|254 +/- 8 Ma (K-Ar biotite: Green, 1975).||||Pale grey, medium- to fine-grained biotite-hornblende granite; medium-grained biotite granite with local miarolitic cavities in south.|
27993|Mena Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group||||||
27993|Mena Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p36|||Of Ebagoola Suite (Kintore Supersuite). Comprises a mafic phase and a felsic phase. Both intrude Dinah Formation and Sugarbag Creek Quartzite, and the mafic phase also intrudes Morehead Granite. Pale grey to white uneven-gr. biotite-muscovite granites.||||||07-APR-15
27993|Mena Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
75748|Menilden Creek Tonalite|68679|5|Briefly described|p362|Pennsylvanian|Pennsylvanian|Northern Connors Subprovince.|308.2 +/- 7.1 Ma  (SHRIMP U-Pb: Allen et al. 1998)|||||
24378|Meringa Basalt|23497|5|Briefly described|Table 1|||of Atherton Subprovince. Age: 986000 BP K-Ar. of Willmott and others, 1988.||||||
24378|Meringa Basalt|23507|5|Briefly described|Map Legend||Quaternary|Age: 0.986 Ma K-Ar whole rock.||||||
24378|Meringa Basalt|42625|5|Briefly described|Map legend|Pleistocene||Reserved.||||||
24378|Meringa Basalt|42810|2|Defined|Table 1 P14|Pleistocene||see also p31.||||||20-AUG-08
24378|Meringa Basalt|60425|6|Mentioned|p42 Tb. 3|Miocene|Miocene|Part of Atherton Basalt grouping.||||||07-FEB-11
24378|Meringa Basalt|72298|5|Briefly described|p792|||A source of groundwater in the Mulgrave River area.||||||
38175|Merriland Suite|23422|5|Briefly described|p175, p213 Table 6.8|||Of Millchester Supersuite.||||||
38175|Merriland Suite|62521|5|Briefly described|p55|||Includes Merriland Tonalite. Geological Province: Ravenswood Batholith.||||||14-JAN-08
38175|Merriland Suite|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.||Millchester Supersuite.|||Mostly medium-K granodiorites to tonalites.|
23788|Merriland Tonalite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
23788|Merriland Tonalite|23422|5|Briefly described|p191, p213 Table 6.8|Middle Devonian|Silurian|||||||
23788|Merriland Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 461. I-Type.||||||
23788|Merriland Tonalite|42633|5|Briefly described|Table 1 P7|||Reserved.||||||
23788|Merriland Tonalite|42750|2|Defined|p45, p42|Early Devonian|Late Silurian|||||||
23788|Merriland Tonalite|43093|4|Described|Appendix 1|Early Devonian|Silurian|Middle Silurian to Early Devonian age.||||||
23788|Merriland Tonalite|43259|4|Described|Appendix 1,p49.|Early Devonian|Late Silurian|||||||
23788|Merriland Tonalite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23788|Merriland Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Merriland ton.||Unit in Millchester Supersuite.||||
35193|Mia Mia Igneous Complex|23042|6|Mentioned|p97 Fig 2||Carboniferous|||||||
35193|Mia Mia Igneous Complex|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Sheared and strongly foliated, commonly altered, fine to medium grained hornblende biotite granodiorite and granite.||||||
35193|Mia Mia Igneous Complex|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35193|Mia Mia Igneous Complex|61916|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Sheared and strongly foliated, commonly altered, fine- to medium-grained hornblende-biotite granodiorite and granite; medium-grained, equigranular biotite leucogranite; sporadic coarse-grained leucogabbro; common rhyolitic to andesitic dykes.||||||
35193|Mia Mia Igneous Complex|61917|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Sheared and strongly foliated, commonly altered, fine to medium-grained hornblende-biotite granodiorite and granite; medium-grained, equigranular biotite leucogranite; sporadic coarse-grained leucogabbro; common rhyolitic to andesitic dykes||||||
35193|Mia Mia Igneous Complex|65388|3|Fully described|p373-375, p135, 362, 364, 365, 392, 443|Early Permian|Late Carboniferous|New name. Northern Connors Arch. Southern Urannah Batholith. Probable age given. Interpreted to be bounded by fault or shear zones. May be intruded by Doraville Granodiorite. Medium-grained, equigranular quartz diorite or tonalite; cream to light grey, fine to medium grained, equigranular biotite granite.||||||
25233|Mica Creek Pegmatite|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier.||||||
25233|Mica Creek Pegmatite|32818|6|Mentioned|p21|||Age||||||
25233|Mica Creek Pegmatite|42503|6|Mentioned|p334|||||||||
25233|Mica Creek Pegmatite|61936|5|Briefly described|p201|||Emplacement during both 1532+/-7 and 1480+/-14Ma periods. Geological Province: Western Fold Belt, Mount Isa Inlier.||||||09-FEB-09
25233|Mica Creek Pegmatite|72297|5|Briefly described|p702, p718|||A phase of the Sybella Granite. Contains tantalite and columbite as well as beryl and mica.|||||Contains beryl crystals up to 1m long and 0.3m wide in dykes and veins.|
29613|Middle Branch Creek Suite|43005|5|Briefly described|p215|||||||||
25235|Middle Creek Sandstone Member|23393|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Of Mullera Formation.||||||
25235|Middle Creek Sandstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Mullera Formation.  ||||||
25235|Middle Creek Sandstone Member|26310|2|Defined|p4, 10, 15|Proterozoic|Proterozoic|Of the Mullera Formation. Quartzitic sandstone, siltstone, shale. Maximum Thickness: 480 feet. Type section in text.||||||
25235|Middle Creek Sandstone Member|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mullera Formation (South Nicholson Group).  Grey and light brown, massive to flaggy, fine to medium sandstone,with some interbedded sitlstone and shale.||||||10-JAN-05
25235|Middle Creek Sandstone Member|39497|4|Described|p15|||See also p5.||||||06-NOV-06
25235|Middle Creek Sandstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25235|Middle Creek Sandstone Member|44482|14|Not recorded|p.9|||(E53-12).||||||
25235|Middle Creek Sandstone Member|44483|5|Briefly described|map legend|||Defn. on Tech.File E/533-12. Upper (?) Proterozoic.||||||
25235|Middle Creek Sandstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Mullera Formation.||||||
25235|Middle Creek Sandstone Member|45166|5|Briefly described|p33|||||||||
25235|Middle Creek Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Mullera Formation.||||||
25235|Middle Creek Sandstone Member|65337|4|Described|p9 Fig.5, p38 Table 5, pp59-60.|Mesoproterozoic|Mesoproterozoic|Southeast MOUNT DRUMMOND area. Formerly the Mistake Creek Sandstone Member. Thickness to 70 m of shallow-marine intertidal and shoreface, above fair-weather wave-base, deposits.||Unit in Mullera Formation.|||White, silicified, fine-grained, sublithic glauconitic sandstone with distinctive decimetre-scale amalgamated trough cross-beds defined by hematite (altered glauconite) dustings on foresets.|
25235|Middle Creek Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin||South Nicholson Group|||Sandstone; siltstone, shale|
25235|Middle Creek Sandstone Member|67539|6|Mentioned|p15, p15 Fig.8|||||Of the Mullera Formation.||||
25235|Middle Creek Sandstone Member|68146|6|Mentioned|p196|||||Mullera Formation||||
25235|Middle Creek Sandstone Member|69434|5|Briefly described|p19:2, 7|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. Shallow-marine intertidal and shoreface deposits, above fair-weather wave base.||Mullera Formation.|||White, silicified, fine +/- medium, sublithic glauconitic sandstone with distinctive decimetre-scale amalgamated trough cross-beds defined by haematite dustings on foresets.|12-JUL-16
25235|Middle Creek Sandstone Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT).||Mullera Formation.||||
25235|Middle Creek Sandstone Member|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Middle Creek, within Mullera [Formation]. South Nicholson Basin.||||||29-NOV-17
25235|Middle Creek Sandstone Member|71369|5|Briefly described|p5-6, p37, p42-44, p48|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960). South Nicholson Basin. Up to 150m thick. Progradational deposits.||Mullera Formation.|||A series of quartz-rich, dark-speckled resistant sandstone units, each 5-10m thick, separated by laminated and thin-bedded mudstone.|
25235|Middle Creek Sandstone Member|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone Member|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Mullera Formation.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone Member|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as located in the central and eastern parts of the South Nicholson Basin.||Probably Mullera Formation.||||
25235|Middle Creek Sandstone Member|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|||mid- Mullera Formation, Accident Subgroup||||
25235|Middle Creek Sandstone Member|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin.||Mullera Formation||||
25235|Middle Creek Sandstone Member|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the central part of the South Nicholson Basin.||Mullera Formation,  Accident Subgroup||Shown as within upper Mullera Formation.|Includes sandstone.|
25235|Middle Creek Sandstone Member|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||Mullera Formation, Accident Subgroup, South Nicholson Group||||
25235|Middle Creek Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. (Relationship between Mullera Formation and Middle Creek Sandstone Member is not clear in Fig.1.2.)||Mullera Formation, Accident Subgroup, South Nicholson Group||Underlain(?) by Train Range Ironstone. Overlain(?) by Tidna Sandstone.||
25235|Middle Creek Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Aquitard with potential shale gas/oil play.||Mullera Formation, Accident Subgroup, South Nicholson Group||||
30203|Middle Mountain Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Parent: McBride Group. Geological Province: Georgetown Region.||||||08-JUL-15
30203|Middle Mountain Basalt|23619|4|Described|p28 table 1||Pleistocene|Of the McBride Basalt Group in the McBride Basalt Province.||||||
30203|Middle Mountain Basalt|43113|4|Described|Table 1 p17|||of McBride Basalt Group.||||||
30203|Middle Mountain Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
30203|Middle Mountain Basalt|68576|6|Mentioned|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30203|Middle Mountain Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pleistocene|Pleistocene|McBride Basalt Province.|0.89 Ma|||||
34982|Middlemount seam|23034|6|Mentioned|24|||Parent Rangal Coal Measures. Max thickness 7.5 m||||||
36420|Midway Creek Granodiorite|23617|4|Described|Table 2 p16|Permian|Late Carboniferous|Also see p26. Intrudes the Poison Creek Granite. Kennedy Province.||||||
36420|Midway Creek Granodiorite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36420|Midway Creek Granodiorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
22333|Milky Granodiorite|23032|5|Briefly described|p40|||||||||
22333|Milky Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
22333|Milky Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
22333|Milky Granodiorite|43480|2|Defined|7-33|Devonian|Silurian|||||||
22333|Milky Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Strongly foliated and schleiren-banded, pink to greyish-pink,  fine- to medium-grained, porphyritic muscovite-biotite granodiorite and granite, with alkali feldspar phenocrysts to 1.5 cm.||||||08-DEC-08
22333|Milky Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Strongly foliated and schlieren banded, pink to greyish-pink, fine- to medium-grained, porphyritic muscovite-biotite granodiorite and granite, with alkali feldspar phenocrysts to 1.5 cm.|
22333|Milky Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
23791|Millchester Creek Tonalite|22611|6|Mentioned|P195||Silurian|||||||
23791|Millchester Creek Tonalite|22847|3|Fully described|p 49|Silurian||||||||
23791|Millchester Creek Tonalite|23062|6|Mentioned|260|||||||||
23791|Millchester Creek Tonalite|23422|5|Briefly described|p176, p213 Table 6.8|Silurian|Silurian|Of Merriland Suite.||||||
23791|Millchester Creek Tonalite|23429|5|Briefly described|Fig 13.25(a) p446|||||||||
23791|Millchester Creek Tonalite|23431|5|Briefly described|p537|||||||||
23791|Millchester Creek Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 472. I-Type.||||||
23791|Millchester Creek Tonalite|41659|5|Briefly described|p364|||||||||
23791|Millchester Creek Tonalite|41668|3|Fully described|p33|||||||||
23791|Millchester Creek Tonalite|42054|6|Mentioned|p272|||||||||
23791|Millchester Creek Tonalite|42633|5|Briefly described|Table 1 P9|||||||||
23791|Millchester Creek Tonalite|42750|2|Defined|p40|Middle Silurian||age of 425 +/- 4 Ma.||||||
23791|Millchester Creek Tonalite|43093|4|Described|Appendix 1|||Rb/Sr age of 425+/-2Ma.||||||
23791|Millchester Creek Tonalite|43259|4|Described|Appendix 1,p50.|Early Devonian|Late Silurian|Rb-Sr ages are 425+/-2 & 426+/-2 Ma.||||||
23791|Millchester Creek Tonalite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23791|Millchester Creek Tonalite|50552|5|Briefly described|p1048 Fig.2||Late Silurian|In Lolworth-Ravenswood Terrane.||||||24-NOV-04
23791|Millchester Creek Tonalite|62074|5|Briefly described|p3|||Charters Towers town area. Hosts some of the major gold lodes in the goldfield.|c.426 Ma (Huttton and Rienks, 1997).|||Intrudes Towers Hill Granite.||
23791|Millchester Creek Tonalite|62075|6|Mentioned|p11 Fig.3, p15 Fig.7|Silurian|Silurian|Appears as Millchester Creek tonalite.||||||
23791|Millchester Creek Tonalite|62521|5|Briefly described|p7 Tb.1, p55|||Of Millchester Creek Supersuite. Age: 426+/-2Ma (Rb-Sr). Geological Province: Ravenswood Batholith. Medium-grained biotite-hornblende granodiorite and tonalite. See also p21.||||||14-JAN-08
23791|Millchester Creek Tonalite|68576|5|Briefly described|Q_11: p41-42|||Charters Towers. Forms the low-lying country at the foot of Towers Hill and through much of the city. Abbreviated to Millchester Tonalite on p42.|||||Hornblende-biotite tonalite.|
34670|Millchester Supersuite|22847|5|Briefly described|p 13|||||||||
34670|Millchester Supersuite|23422|5|Briefly described|p175, p213 Table 6.8|Late Silurian|Silurian|||||||
34670|Millchester Supersuite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
34670|Millchester Supersuite|62075|5|Briefly described|p10, p15 Fig.7|||Also includes Beasley Creek, Heathfield West, Merriland, Wellington Springs, Wharleys and Yulga Tonalites. Medium to high-K calc-alkaline. Hosts some of the gold veins in the Charters Towers District.|||Boatswain, Casey Spring Creek, Centauri, Crescent, Dalmore, Emu Mill, Five Mile Mill, Meadowvale, Molly Darling, Spondulix, Tullegorim, Urdera Granodiorites; Two Mile Granite; see Comments for others.||Oxidised, I-type granitoids.|
34670|Millchester Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Toms Hole and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
34670|Millchester Supersuite|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.|||Riverview, Merriland Suites.||Mostly medium-K granodiorites to tonalites.|
34670|Millchester Supersuite|71031|5|Briefly described|p57|Silurian|Silurian||||Includes the Meadowvale Granodiorite.|Overlain by the Fanning River Group.||
81261|Millungera Basin - quartzite 81261|71382|5|Briefly described|p4, p18, p25, p27, App 3, 4|||Millungera Basin. Intersected in GSQ Julia 1 from 320.05m->500.02m for a total thickness in excess of 179.97m.||||Overlain by the Hooray Sandstone.|Dominantly hematitic fine- to granule-grained quartzite, fine- to coarse-grained quartzose sandstone and micaceous clays.|
31441|Milo beds|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1760Ma. Geological Province:Mount Isa Inlier.||||||07-FEB-11
31441|Milo beds|50332|6|Mentioned|p21|Proterozoic|Proterozoic|Informal name. Of the "Tommy Creek beds".||||||07-FEB-11
31441|Milo beds|50536|5|Briefly described|p1.5, 11.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Tommy Creek Suite. Age: ~1620Ma.||||||
31441|Milo beds|67323|5|Briefly described|GIS attrib tbl, p17, p36, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Tommy Creek Domain. Isa Superbasin. Low magnetic, but high K, responses. A range of ages is given. It appears to be one of the youngest parts of the succession in the Mount Isa Inlier.|1618 +/- 4 Ma (Hill et al., 1992).|||Unconformably overlies Corella Formation and Tommy Creek Microgranite.|Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|67539|5|Briefly described|p12|Statherian|Statherian|Suggested that the ~ 1620 Ma age previously determined by Rod Page may be valid.|~ 1620 Ma|||Probably unconformable over Tommy Creek Microgranite, rather than intruded by it.||
31441|Milo beds|68146|5|Briefly described|p2, p6, p121-126, p198, p211|||Tommy Creek Domain. Several features of the zircons dated are listed as evidence that this age from volcanic zircons is probably close to true depositional age. Whole-rock Sm-Nd isotopic data tabulated.|1615 +/- 5 Ma maximum depositional age.||||A package of clastic and volcanogenic metasediments, including biotite metapelite.|
31441|Milo beds|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
31441|Milo beds|69056|5|Briefly described|p2, p4, p6, p13, p18, p23, p28, p56|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Tommy Creek Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area. Age range from Space-Time Plot; the text also gives ~1660-1610 Ma age range. Modelling values listed.|~1630 - ~1605 Ma.|||Correlated with upper part of McNamara Group.|Impure carbonates, carbonaceous shales and volcaniclastics.|
31441|Milo beds|69591|5|Briefly described|p29, p43, p46-47, p54, p108|Paleoproterozoic|Paleoproterozoic|Tommy Creek Domain. Shallow carbonate shelf to deep marine deposits. Several ages given; the youngest is 1610 +/- 6 Ma (Carson et al., 2011).|1615 +/- 4 Ma (Carson et al., 2011).|||Nonconformably overlies Tommy Creek Microgranite. Correlated with upper McNamara Group, and Term or Lawn Supersequences.|Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Tremolitic marble and calc-silicate rocks, mica schist, graphitic schist, quartzite, porphyritic mafic to intermediate lava and volcaniclastic rocks, metarhyolite and felsic volcaniclastic rocks.|
31441|Milo beds|72889|6|Mentioned|p6 Fig.i.|||||||||
31441|Milo beds|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
31441|Milo beds|73553|6|Mentioned|p187|||||||||
75666|Milwarra Quartz Diorite|68679|5|Briefly described|p362|Mississippian|Mississippian|Northern Connnors Subprovince. Unfoliated.|322.3 +/- 2.1 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75666|Milwarra Quartz Diorite|68901|5|Briefly described|p8, p27-p29, p146|||New England Region. SHRIMP age is interpreted as the age of magmatic crystallisation.|322.3 +/- 2.1 Ma|||Intruded by the Tommy Roundback Granodiorite.|Pale grey, medium-grained, slightly uneven-grained biotite-hornblende quartz diorite, containing traces of titanite.|
75666|Milwarra Quartz Diorite|70673|5|Briefly described|p5, p123|Late Carboniferous|Late Carboniferous|Indistinguishable from ages for adjacent Ward Creek Granodiorite and Tommy Roundback Granodiorite.|322.3 +/- 2.1 Ma (Cross et al., 2012).|||||
75666|Milwarra Quartz Diorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|322+/-2.1 Ma (crystallisation: U-Pb zircon SHRIMP)||||Quartz diorite.|
23796|Mingela Granodiorite|22847|3|Fully described|p 11|Devonian|Ordovician|||||||
23796|Mingela Granodiorite|23422|5|Briefly described|p189,190, p213 Table 6.8|||Of Mingela Suite. See also Mingela Volcanics.  Probably Middle Ordovician to early Silurian.||||||
23796|Mingela Granodiorite|23430|5|Briefly described|p482|||||||||
23796|Mingela Granodiorite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
23796|Mingela Granodiorite|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 90. I-Type.||||||
23796|Mingela Granodiorite|23893|6|Mentioned|p13|||||||||
23796|Mingela Granodiorite|42245|2|Defined|p35|Ordovician||||||||
23796|Mingela Granodiorite|42407|6|Mentioned|p42|||||||||
23796|Mingela Granodiorite|42750|6|Mentioned|p36, p46|||||||||
23796|Mingela Granodiorite|43093|4|Described|Appendix 1|Early Silurian|Late Ordovician|Probable Late Ordovician or Early Silurian age.||||||
23796|Mingela Granodiorite|43259|4|Described|Appendix 1,p21.|Early Devonian|Ordovician|Ordovician and Late Silurian to Early Devonian?||||||
23796|Mingela Granodiorite|43933|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
23796|Mingela Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
23796|Mingela Granodiorite|62075|6|Mentioned|p9 Fig.2|Early Silurian|Late Ordovician|Appears as Mingela granodiorite.||||||
23796|Mingela Granodiorite|68419|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, commonly foliated, medium to coarse-grained biotite-hornblende granodiorite with common enclaves of grey, unfoliated, fine to coarse-grained biotite-hornblende granodiorite.|
23796|Mingela Granodiorite|68420|5|Briefly described|Map Legend|Silurian|Ordovician|Of the Macrossan Province.|||||Grey, commonly foliated, medium to coarse-grained biotite-hornblende granodiorite with common enclaves of grey, unfoliated, fine to coarse-grained biotite-hornblende granodiorite.|
23796|Mingela Granodiorite|68553|6|Mentioned|Map legend|Early Silurian|Ordovician|This unit, as well as the Columbia Creek Supersuite (in part) and various Early Silurian ungrouped plutonic units, are mapped under the same symbol, OSgm.||||||
23796|Mingela Granodiorite|68731|6|Mentioned|p150|||Shows pervasive ductile shear - interpreted as syn-tectonically emplaced. See also Mingella Granodiorite.||||||
23796|Mingela Granodiorite|68900|6|Mentioned|p4|Early Silurian|Ordovician|Drummond Basin.||||||
38238|Mingela Suite|23422|4|Described|p213 Table 6.8|||||||||
38238|Mingela Suite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
38100|Mingham Formation|24382|5|Briefly described|Map legend|Pleistocene|Pleistocene|||||||
38100|Mingham Formation|63821|5|Briefly described|p26|Tertiary|Tertiary|Comprises polymictic boulder to pebble conglomerate and sandstone.||||||07-FEB-11
82771|Mingimarny Monzogranite|71628|3|Fully described|p19: 103-104|||Originally the Mingimarny Granite of Purdy et al. (2005); p19-103 has it as 2007. Name is from either the parish or a local watercourse. Occurs as a small (~5 km2) stock 20 km S of Millmerran. The type locality is MGA 326796 6897250. Resistant; crops out as extensive pavements and scattered boulders. Geochemistry described.|260.1 +/- 2.4 Ma (SHRIMP: Cross et al., 2009).|Mingimarny Suite.||Is overlain locally by Marburg Formation.|Pale grey or white to buff, moderately porphyritic, leucocratic biotite monzogranite. I-type.|
74063|Mingimarny Suite|63748|5|Briefly described|p26-27|||Of the Bullaganang Supersuite.||||||07-FEB-11
74063|Mingimarny Suite|68679|5|Briefly described|p457, p459-460|Permian|Permian|Northern New England Batholith.|~260 Ma.|Stanthorpe Supersuite.|Mingimarny Granite.|||
74063|Mingimarny Suite|71628|5|Briefly described|p19:103|||Donchak et al. (2007) assigned this unit and its constituent the Mingimarny Granite (now Monzogranite) to the Bullaganang Supersuite; subsequent dating invalidates that.|||Mingimarny Monzogranite.|||
23797|Mingo Granite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
23797|Mingo Granite|39505|6|Mentioned|p178|||||||||
23797|Mingo Granite|39997|6|Mentioned|p165|||||||||
23797|Mingo Granite|40919|6|Mentioned|Fig.2|||||||||
23797|Mingo Granite|41778|2|Defined|Table 1|Permian||Described P372.||||||18-AUG-08
23797|Mingo Granite|42054|6|Mentioned|p273|||||||||
23797|Mingo Granite|43008|5|Briefly described|map legend|||||||||
23797|Mingo Granite|63821|5|Briefly described|p28|Late Permian|Early Permian|Age: 261+/-2Ma (K-Ar biotite). Biotite granite.||||||07-FEB-11
23797|Mingo Granite|68679|5|Briefly described|p410, p420-422|Permian|Permian|Gayndah-Gladstone belt, southern part of the northern New England Orogen. Late Pemian.|261 +/- 2 Ma (K-Ar: Cranfield and Murray, 1989).|||Intrudes the Good Night beds and Shoalwater Formation. Is overlain by Toogoolawah Group and Aranbanga Volcanic Group. Is adjacent to Wateranga Gabbro and Yenda Granodiorite.|Muscovite-biotite granite, biotite granodiorite, migmatite (probably restitic); separate subunit of diorite, minor biotite granodiorite and granite. Probably S-type.|
23797|Mingo Granite|73197|6|Mentioned|p476 Fig.7, p479|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase. S-type intrusive.|~270-260 Ma||||Intrusives.|
22345|Minnamoolka Granite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
22345|Minnamoolka Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 404. I-Type.||||||
22345|Minnamoolka Granite|23619|4|Described|p39 Table 2|Permian|Carboniferous|Overlying unit McBride Basalt Group. Herbert River Batholith.||||||
22345|Minnamoolka Granite|43113|4|Described|Table 2 p24|Permian|Carboniferous|||||||
22345|Minnamoolka Granite|43253|5|Briefly described|map legend|Permian|Carboniferous|||||||
22345|Minnamoolka Granite|43259|4|Described|Appendix 1,p45.|Permian|Carboniferous|||||||
22346|Minnemore Granodiorite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes the Tate Batholith undivided. Geological Province: Georgetown Region.||||||02-JUL-15
22346|Minnemore Granodiorite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
22346|Minnemore Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 364. I-Type.||||||
22346|Minnemore Granodiorite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22346|Minnemore Granodiorite|23624|4|Described|p15|Permian|Carboniferous|Parent: Ootann Supersuite.||||||02-JUL-15
22346|Minnemore Granodiorite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
22346|Minnemore Granodiorite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, fine- to medium-grained hornblende-biotite granodiorite and fine-grained biotite-hornblende granodiorite.|
22346|Minnemore Granodiorite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, fine- to medium-grained hornblende-biotite granodiorite and fine-grained biotite-hornblende granodiorite.|
79636|Minoru Plains Volcanics|70821|6|Mentioned|p12|||Not encountered in outcrop or boreholes in this study. Characterised by linear trends of moderate to high magnetic intensity.||||||
79636|Minoru Plains Volcanics|71251|6|Mentioned|p3|||N and S of Cunnamulla. Map symbol ( Emp) implies Cambrian age suspected or inferred.||||||26-APR-18
79636|Minoru Plains Volcanics|71864|6|Mentioned|p3|||||||||
79428|Minya Leucogranite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.|||||Muscovite-tourmaline pegmatite and fine to coarse-grained pink leucogranite.|05-MAY-16
79428|Minya Leucogranite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||||Muscovite-tourmaline pegmatite and fine to coarse grained pink leucogranite.
|
79428|Minya Leucogranite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||||Muscovite-tourmaline pegmatite and fine to coarse grained leucogranite.|20-JAN-22
79428|Minya Leucogranite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Soldiers Cap Domain.|||||Muscovite-tourmaline pegmatite and fine-coarse grained leucogranite.
|
26033|Miriam Vale Granodiorite|9194|5|Briefly described|Map legend|Early Triassic|Late Permian|Biotite granodiorite, adamellite, quartz diorite, marginal pegmatite and gneiss; rare gabbro.  Intrudes Curtis Island Group.||||||12-JUL-04
26033|Miriam Vale Granodiorite|24420|4|Described|p8|Late Triassic|Late Permian|||||||
26033|Miriam Vale Granodiorite|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
26033|Miriam Vale Granodiorite|24490|5|Briefly described|Map Legend|Late Permian|Permian|Granodiorite, diorite, monzogranite.||||||04-SEP-08
26033|Miriam Vale Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgmv].  Hornblende quartz diorite, hornblende-biotite tonalite, biotite-hornblende granodiorite, local olivine-hornblende-augite gabbro, hornblende-biotite granite.||||||
26033|Miriam Vale Granodiorite|30451|2|Defined|p83|Late Paleozoic|Late Paleozoic|||||||07-NOV-08
26033|Miriam Vale Granodiorite|30655|3|Fully described|p35|||||||||
26033|Miriam Vale Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
26033|Miriam Vale Granodiorite|31658|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26033|Miriam Vale Granodiorite|31659|6|Mentioned|Table 4|||||||||
26033|Miriam Vale Granodiorite|32358|4|Described|p17|||Table 4||||||
26033|Miriam Vale Granodiorite|32882|6|Mentioned|p380|||||||||
26033|Miriam Vale Granodiorite|33142|4|Described|p3|||Permo-Triass||||||
26033|Miriam Vale Granodiorite|33728|6|Mentioned|Fig.1|||||||||
26033|Miriam Vale Granodiorite|34955|6|Mentioned|p227|||||||||
26033|Miriam Vale Granodiorite|35043|6|Mentioned|p78|||||||||
26033|Miriam Vale Granodiorite|36045|6|Mentioned|p334|||||||||
26033|Miriam Vale Granodiorite|36488|6|Mentioned|p4|||||||||
26033|Miriam Vale Granodiorite|36926|6|Mentioned|p168|||||||||
26033|Miriam Vale Granodiorite|38447|6|Mentioned|Map legend|Triassic|Permian|Permian to Triassic||||||
26033|Miriam Vale Granodiorite|39445|5|Briefly described|Table 12|||||||||
26033|Miriam Vale Granodiorite|39505|6|Mentioned|p167|||||||||
26033|Miriam Vale Granodiorite|39632|6|Mentioned|p221|||||||||
26033|Miriam Vale Granodiorite|40247|6|Mentioned|p207|||||||||
26033|Miriam Vale Granodiorite|40786|5|Briefly described|p403|||||||||
26033|Miriam Vale Granodiorite|42895|6|Mentioned|Fig.7 P60|||||||||
26033|Miriam Vale Granodiorite|50190|6|Mentioned|p11|||||||||
26033|Miriam Vale Granodiorite|50207|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
26033|Miriam Vale Granodiorite|68008|3|Fully described|p2, p199, p324-329, p371-372, p388|Permian|Permian|See also p413-414, p416, p418, p491. Dear et al. (1971), for a granodiorite-tonalite-diorite batholith 50 x 15 km. Named after the township of Miriam Vale. No type area; there is no single representative lithology. Named the Jackass Gabbro on the Miriam Vale 100k sheet. Low topography; sparse outcrop. Geochemistry compared with Castletower Granite: some features of both are similar to Winterbourne and Coulston Volcanics, and to Robert and Molangul Granites; also similar to Mount Seaview Igneous Complex. May be mid-Permian.||||Intrudes Wandilla, Shoalwater Formations. Is intruded by Castletower Granite, Norton and Bororen Tonalites. Is overlain nonconformably by Bobby and Coulston Volcanics.|Diverse lithologies described in some detail, including medium-grained hornblende-biotite syenogranite, hornblende-quartz microdiorite, gabbro, quartz diorite, granodiorite.|
26033|Miriam Vale Granodiorite|68679|5|Briefly described|p420, p422, p431|||Ellis and Whitaker (1976). Gayndah-Gladstone belt, northern New England Orogen. Formerly very extensive; many units have been divided from this formation.||||||
26033|Miriam Vale Granodiorite|73450|6|Mentioned|p7, p16, p18, p20, p22|||Previously mapped to include Foreshores Granite, John Clifford Road Granite, Grevillea Granite, Molangul Granite, and Borilla Granite (Ellis, 1974).||||||
36188|Mission Beach Granite Complex|23497|5|Briefly described|Table 1|Late Ordovician|Early Ordovician|Of Macrossan Province. Granite which intrudes Tam O'Shanter Granite has yielded a U-Pb SHRIMP age of 463+/-7Ma. Intrudes Barnard Metamorphics, and Tam O'Shanter Granite. Faulted against Hodgkinson Fm rocks.||||||10-AUG-05
36188|Mission Beach Granite Complex|23507|5|Briefly described|Map Legend|Late Ordovician|Early Ordovician|||||||
36188|Mission Beach Granite Complex|60425|3|Fully described|p62 Tb. 4|Late Ordovician|Ordovician|Of S. Wegner. Comprises several informal units - Garners diorite and Timana diorite, South mission granite. Age: ~460Ma; 463+/-7Ma (SHRIMP). I-type granites probably. Intrudes Barnard metamorphics and Tam O'Shanter Granite. See also p6, p8, p11.||||||07-FEB-11
36188|Mission Beach Granite Complex|68731|6|Mentioned|p159, p162|Late Ordovician|Middle Ordovician||459 +/- 8 Ma, U-Pb SHRIMP (Bultitude et al. 1999)|||Extensively intrudes the Barnard Metamorphics.||
36188|Mission Beach Granite Complex|69030|5|Briefly described|p6|Ordovician|Ordovician|Barnard Province.|459 +/- 8 Ma (SHRIMP).|||||
36188|Mission Beach Granite Complex|70033|5|Briefly described|p5, p52 Fig 8.1, p58, p61|Ordovician|Ordovician|BB1715; 459 +/- 8 Ma; SHRIMP; M. Fanning, ANU, 1992, unpubl. report to GSQ; see Bultitude and Champion 2013.||||Intrudes Barnard Metamorphics.||
36188|Mission Beach Granite Complex|73425|6|Mentioned|p16|Late Ordovician|Late Ordovician|Barnard Province, Thomson Orogen. Metamorphosed in the Silurian.||||||
36188|Mission Beach Granite Complex|73595|6|Mentioned|p1134|Silurian|Ordovician|||||||
22352|Mistake Granodiorite|23032|5|Briefly described|p40|||||||||
22352|Mistake Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
22352|Mistake Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
22352|Mistake Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
22352|Mistake Granodiorite|43480|2|Defined|7-29|Devonian|Silurian|||||||
22352|Mistake Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Foliated grey to buff-grey, porphyritic muscovite-biotite granodiorite, with common alkali feldspar phenocrysts to 3 cm.||||||08-DEC-08
22352|Mistake Granodiorite|65003|6|Mentioned|p22||||||||Foliated grey, porphyritic, alkali feldspar granodiorite.|30-MAR-12
22352|Mistake Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Foliated grey to buff-grey, porphyritic muscovite-biotite granodiorite, with common alkali feldspar phenocrysts to 3 cm.|
22352|Mistake Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated grey to buff-grey, porphyritic muscovite-biotite granodiorite, with common alkali feldspar phenocrysts to 3 cm.|
22352|Mistake Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated grey to buff-grey, porphyritic muscovite-biotite granodiorite, with common alkali feldspar phenocrysts to 3 cm.|
22352|Mistake Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
27198|Mistletoe Granite|9539|5|Briefly described|Map legend|Proterozoic|Proterozoic|Dark grey foliated biotite granite with schlieren and sporadic muscovite; xenoliths characteristic. Age: Mid-Proterozoic?||||||07-JUL-04
27198|Mistletoe Granite|23291|5|Briefly described|p88 Tb. 3.7, p31|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
27198|Mistletoe Granite|23430|5|Briefly described|Table 14.2 p460.||Mesoproterozoic|Zircon  crystallisation 1544 +/- 7 Ma. Forsayth Subprovince.||||||
27198|Mistletoe Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 814. S-Type.||||||
27198|Mistletoe Granite|23616|5|Briefly described|p64|||SHRIMP U-Pb 1544+/-7 Ma. Of Forsayth Supersuite.||||||
27198|Mistletoe Granite|24197|5|Briefly described|p17, p77|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Contains cordierite and metasedimentary xenoliths are common. Age: 1550+/-6Ma. Geological province: Georgetown Inlier. See also p79 Tb. 9.1.||||||07-FEB-11
27198|Mistletoe Granite|24485|5|Briefly described|p59|Mesoproterozoic|Mesoproterozoic|Age: 1544 +/- 7Ma (U-Pb SHRIMP zircon). Parent: Forasyth Supersuite||||||
27198|Mistletoe Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27198|Mistletoe Granite|33909|2|Defined|p229|Proterozoic|Proterozoic|||||||
27198|Mistletoe Granite|35214|6|Mentioned|p7|||||||||
27198|Mistletoe Granite|37570|4|Described|p118|||See also p113.||||||16-JAN-07
27198|Mistletoe Granite|39445|5|Briefly described|Table 2|||See also p45.||||||16-JAN-07
27198|Mistletoe Granite|39687|6|Mentioned|p3|||||||||
27198|Mistletoe Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27198|Mistletoe Granite|41272|6|Mentioned|M 1of1 L04|||||||||
27198|Mistletoe Granite|43060|5|Briefly described|p78|||Age of 1544+/-7 Ma. Of Forsayth Supersuite.||||||16-JAN-07
27198|Mistletoe Granite|43083|5|Briefly described|p114|||U-Pb age of 1554+/-7 Ma.||||||16-JAN-07
27198|Mistletoe Granite|43087|5|Briefly described|p8|||U-Pb zircon age of 1544 +/-7 Ma.||||||
27198|Mistletoe Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic. U-Pb zircon age is 1550+/-7 Ma.||||||03-DEC-13
27198|Mistletoe Granite|43664|6|Mentioned|p93|||||||||
27198|Mistletoe Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
27198|Mistletoe Granite|50537|5|Briefly described|p1.2, 1.4, 2.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite. Age: 1550-1544 +/- 7Ma (U-Pb).||||||
27198|Mistletoe Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Muscovite-biotite granite.||||||05-JUL-04
27198|Mistletoe Granite|61258|6|Mentioned|p386|Mesoproterozoic|Mesoproterozoic|Age: 1558+/-4Ma (Black and McCulloch 1990) and 1544+/-7Ma.||||||
27198|Mistletoe Granite|63866|5|Briefly described|p77|Calymmian|Calymmian||1544 +/- 7 ma (U-Pb zircon, TIMS)|Forsayth Supersuite||||
27198|Mistletoe Granite|66800|6|Mentioned|p926.||||1544 +/- 7 Ma (Black & McCulloch 1990).|||||
27198|Mistletoe Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, variably foliated, locally nebulitic, medium-grained muscovite-biotite granite, commonly with abundant mafic clots and schlieren and metamorphic xenoliths.|
27198|Mistletoe Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, variably foliated, locally nebulitic, medium-grained muscovite-biotite granite, commonly with abundant mafic clots and schlieren and metamorphic xenoliths and screens.|
27198|Mistletoe Granite|68576|5|Briefly described|Q_11: p22 Fig.20, p24-25|Mesoproterozoic|Mesoproterozoic|Georgetown area. Part of Forsayth Batholith.|1544 +/- 7 Ma (SHRIMP U-Pb zircon).||||Medium-grained muscovite-biotite granite containing abundant biotite-rich schlieren and xenoliths of gneiss, amphibolite and vein quartz which are interpreted as restite. Strongly peraluminous; S-type.|
27198|Mistletoe Granite|69591|5|Briefly described|p81-82|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith. Small (0.01-1.0 km2) plutons.||Forsayth Supersuite.|||Migmatitic granite bodies. Enclaves and locally abundant metasedimentary xenoliths are common.|
27198|Mistletoe Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province. Age determination by U-Pb zircon (unspecified).|1544+/-7 Ma (crystallisation).||||Granite.|
27198|Mistletoe Granite|73527|6|Mentioned|p2|||Georgetown Inlier, central domain.||Forsayth Supersuite||||
27198|Mistletoe Granite|73642|5|Briefly described|p4 Tb.1, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier.|1544+/-14 Ma|Forsayth Supersuite||||
27198|Mistletoe Granite|75079|6|Mentioned|p3, 6, 10-12|Mesoproterozoic|Mesoproterozoic|Northeast Queensland. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|~1550 Ma.|Forsayth Supersuite.||||
25245|Mitakoodi Quartzite|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Includes: Wakeful Metabasalt Member. Of the Malbon Group. Overlies Marraba Volcanics. Underlies Overhang Jaspilite.||||||18-JAN-07
25245|Mitakoodi Quartzite|22461|6|Mentioned|Fig 1 p464|||Also see Fig 2 p466.||||||
25245|Mitakoodi Quartzite|22747|6|Mentioned|Table1,p7|||Correlates in part with Eastern Creek Volcanics||||||
25245|Mitakoodi Quartzite|23064|6|Mentioned|136|||||||||
25245|Mitakoodi Quartzite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1756+/-3Ma.||||||18-JAN-07
25245|Mitakoodi Quartzite|23458|6|Mentioned|p129|||Rocks referred to as correlates only.||||||
25245|Mitakoodi Quartzite|24197|6|Mentioned|p92|||Interbedded with felsic volcanics coeval with the intrusive Burstall Suite.||||||07-FEB-11
25245|Mitakoodi Quartzite|24254|5|Briefly described|p21|Proterozoic|Proterozoic|Geological Province: Eastern Fold Belt, Mount Isa Inlier. Age: ca. 1760-1755 Ma (SHRIMP U-Pb).||||||
25245|Mitakoodi Quartzite|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlain by Ballara Quartzite. Geological Province: Eastern Fold Belt.||||||
25245|Mitakoodi Quartzite|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25245|Mitakoodi Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Malbon Group.||||||25-AUG-04
25245|Mitakoodi Quartzite|30530|4|Described|p516|||Revision of name.||||||
25245|Mitakoodi Quartzite|30531|6|Mentioned|p15|||Also mention p17.||||||06-FEB-07
25245|Mitakoodi Quartzite|31366|6|Mentioned|p3|||L. Proterozoic||||||
25245|Mitakoodi Quartzite|32660|5|Briefly described|Table 5|||||||||
25245|Mitakoodi Quartzite|32959|6|Mentioned|Fig.21|||||||||
25245|Mitakoodi Quartzite|33214|6|Mentioned|Fig.1|||||||||
25245|Mitakoodi Quartzite|33561|6|Mentioned|p102|||||||||
25245|Mitakoodi Quartzite|33900|5|Briefly described|p16|||Mention p15.||||||18-JAN-07
25245|Mitakoodi Quartzite|34061|6|Mentioned|p54|||||||||
25245|Mitakoodi Quartzite|35074|6|Mentioned|Fig.2|||||||||
25245|Mitakoodi Quartzite|35117|6|Mentioned|p37|||||||||
25245|Mitakoodi Quartzite|35286|6|Mentioned|Fig.17|||||||||
25245|Mitakoodi Quartzite|35295|6|Mentioned|p603|||||||||
25245|Mitakoodi Quartzite|37568|5|Briefly described|p81|||||||||
25245|Mitakoodi Quartzite|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25245|Mitakoodi Quartzite|37862|6|Mentioned|p587|||||||||
25245|Mitakoodi Quartzite|38234|4|Described|p104|||||||||
25245|Mitakoodi Quartzite|38276|6|Mentioned|Fig.1|||||||||
25245|Mitakoodi Quartzite|38350|4|Described|p10|||||||||
25245|Mitakoodi Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25245|Mitakoodi Quartzite|38834|6|Mentioned|p162|||||||||
25245|Mitakoodi Quartzite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Malbon Group.||||||18-JAN-07
25245|Mitakoodi Quartzite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25245|Mitakoodi Quartzite|39445|6|Mentioned|p36|||See also P42 AND Table 2. Shoreline deposit.||||||06-FEB-07
25245|Mitakoodi Quartzite|39496|4|Described|p5|||||||||
25245|Mitakoodi Quartzite|39622|6|Mentioned|p19|||||||||
25245|Mitakoodi Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
25245|Mitakoodi Quartzite|40623|5|Briefly described|p95|||||||||
25245|Mitakoodi Quartzite|40840|6|Mentioned|Map legend|||||||||
25245|Mitakoodi Quartzite|41306|4|Described|p6|||||||||
25245|Mitakoodi Quartzite|41464|6|Mentioned|Map legend|Proterozoic||||||||
25245|Mitakoodi Quartzite|41556|6|Mentioned|Map legend|Proterozoic||||||||
25245|Mitakoodi Quartzite|41568|6|Mentioned|p5|||||||||
25245|Mitakoodi Quartzite|41761|5|Briefly described|p285|||||||||
25245|Mitakoodi Quartzite|41791|5|Briefly described|p248|||||||||
25245|Mitakoodi Quartzite|41978|6|Mentioned|p501|||||||||
25245|Mitakoodi Quartzite|41979|6|Mentioned|p527|||||||||
25245|Mitakoodi Quartzite|42565|5|Briefly described|Table 1 P5, P3|||||||||
25245|Mitakoodi Quartzite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Malbon Group. Sandstone, minor siltstone.||||||09-FEB-09
25245|Mitakoodi Quartzite|42806|6|Mentioned|p123|||Discussion of Williams (1989).||||||
25245|Mitakoodi Quartzite|42807|6|Mentioned|p125|||||||||
25245|Mitakoodi Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
25245|Mitakoodi Quartzite|44271|2|Defined|p29,50,51,60|||Manganese deposit at contact with Marimo Slate.||||||
25245|Mitakoodi Quartzite|44275|14|Not recorded|Map Legend|||||||||
25245|Mitakoodi Quartzite|44276|2|Defined|p11,17,Tb.1,map|||||||||
25245|Mitakoodi Quartzite|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
25245|Mitakoodi Quartzite|44278|2|Defined|Tb.1,map,p6,7||Paleoproterozoic|||||||07-NOV-08
25245|Mitakoodi Quartzite|44279|14|Not recorded|Tb.1|||||||||
25245|Mitakoodi Quartzite|44290|14|Not recorded|p438|||||||||
25245|Mitakoodi Quartzite|44521|14|Not recorded|p37,map|||||||||
25245|Mitakoodi Quartzite|44765|14|Not recorded|p15,16||Paleoproterozoic|||||||07-NOV-08
25245|Mitakoodi Quartzite|44989|2|Defined|p.76|||Tb.III. On many pages. (F54-2,6).||||||
25245|Mitakoodi Quartzite|45136|3|Fully described|p24|||||||||
25245|Mitakoodi Quartzite|45161|4|Described|p40|||||||||
25245|Mitakoodi Quartzite|45166|5|Briefly described|p20|||||||||
25245|Mitakoodi Quartzite|45287|14|Not recorded|p.225,226,231|||||||||
25245|Mitakoodi Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25245|Mitakoodi Quartzite|46962|4|Described|Table 1|||See also Fig.3.||||||
25245|Mitakoodi Quartzite|49009|6|Mentioned|p4|||||||||
25245|Mitakoodi Quartzite|49041|6|Mentioned|Table 4|||||||||
25245|Mitakoodi Quartzite|50100|5|Briefly described|p11, p17|Proterozoic|Proterozoic|Clastic rocks mainly but includes basaltic lavas such as the Wakeful Metabasalt Member.   See also p75.||||||
25245|Mitakoodi Quartzite|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
25245|Mitakoodi Quartzite|50332|5|Briefly described|p16, p18, p89|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Consists mainly of clastic rocks but also includes basaltic lavas (Wakeful Metabasalt Mamber) and felsic porphyry.||||||16-APR-12
25245|Mitakoodi Quartzite|50536|5|Briefly described|p1.1, 5.2, 6.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1756 +/- 3Ma (SHRIMP).||||||16-MAY-13
25245|Mitakoodi Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Malbon Group. Meta-arenite.||||||
25245|Mitakoodi Quartzite|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Eastern Fold Belt.||||||03-JUN-09
25245|Mitakoodi Quartzite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
25245|Mitakoodi Quartzite|61922|5|Briefly described|p8, p9 Fig. 3, p15-16 Figs. 7 and 8|Paleoproterozoic|Paleoproterozoic|Together with Ballara Quartzite and Quilalar Quartzite forms marker horizon within cover sequence 2. Age: ca1755Ma. Has been thrust over Overhang Jaspilite (Bulonga Thrust). Geol. Prov: Mount Isa Inlier/Eastern Fold Belt.||||||07-NOV-08
25245|Mitakoodi Quartzite|61925|4|Described|p57 Fig. 2, p58 Fig. 3, p9 Fig. 4|||Of the Malbon Group. Geological Province: Leichardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||
25245|Mitakoodi Quartzite|61926|5|Briefly described|p70-71|Paleoproterozoic|Paleoproterozoic|Of the Malbon Group. Quartz arenite, feldspathic sandstone, minor calc-silicate. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
25245|Mitakoodi Quartzite|61929|5|Briefly described|p127, p128 Fig. 2|||Of the Mary Kathleen Group? Geological Province: Leichhardt Superbasin.||||||06-FEB-07
25245|Mitakoodi Quartzite|61933|6|Mentioned|p176|||Overlies the Marraba Volcanics.||||||
25245|Mitakoodi Quartzite|63593|6|Mentioned|p288 Fig.2. |||Appears in Fig.2 as Ballara (Mitakoodi) Quartzite.||||||
25245|Mitakoodi Quartzite|63866|6|Mentioned|p62, p65|||||||Overlies the Marraba Volcanics.||
25245|Mitakoodi Quartzite|64248|5|Briefly described|p32-33,p38 Fig.5,p40 Fig.6,p43 Fig.11|Statherian|Statherian|See also p46. Foster and Austin (2008) proposed this unit's age is equivalent with Ballara Quartzite. Shown as BM Quartzite, for Ballara and Mitakoodi Quartzites (p33 Fig.1, p41 Tb. 2), which replace the Double Crossing Metamorphics.|1756 +/- 3 Ma.|||Overlies Marraba Volcanics. Age correlated with Ballara Quartzite. Is overlain by Overhang Jaspilite.||11-DEC-17
25245|Mitakoodi Quartzite|64250|5|Briefly described|p7, p13 figs 4,5, p15, p11 fig 3, p15|||Cloncurry Fold Belt, Mount Isa Inlier. Outcrops to east of Pilgrim Fault with thickness increasing eastwards up to 3000m. Ages refer to limbs of an anticline. Given geochronological and lithological similarities, the two units (Ballara-Mitakoodi Quartzite) are here treated as a single fluvial, near-shore beach, and shallow marine sequence, with this (hopefully temporary) name, and referred to in figure as BM Quartzite (Fig.2, Fig.8).|1755 +/-3 Ma (east); 1756 +/-3 Ma (west).|||Overlies Marraba Volcanics. Is overlain by Corella and Doherty Formations. Equivalent to Ballara Quartzite.|Thick quartzite and sandstone dominated unit (minor metabasalt and felsic porphyry).|12-MAY-14
25245|Mitakoodi Quartzite|64251|5|Briefly described|p52, p62 Fig. 8, p63 Fig. 11, p64|Paleoproterozoic|Paleoproterozoic|Age: 1775Ma (Page 1998). Geological Province: Mount Isa Inlier.||||||05-MAY-09
25245|Mitakoodi Quartzite|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
25245|Mitakoodi Quartzite|65396|4|Described|p7, p15, p17, p77, p82, p84, p169|Statherian|Statherian|See also p173-175, p181-183, p187, p190, p194, p196, p202, p217, p222, p241, p266, p439. Roughly 3000m thick; thins westward towards the Pilgrim Fault. Leichhardt Superbasin. Eastern succession, Cover Sequence 2. With the Mitakoodi Quartzite forms a single regionally extensive sequence. The authors have chosen to combine the Ballara and Mitakoodi Quartzites on the basis of their similar lithologies, ages and outcrop characteristics. Fluvial, near-shore beach, and shallow-marine sequence. Appears as BM Quartzite on p4, p23, 173.|1756 +/- 3 Ma, 1755 +/- 3 Ma|Malbon Group||Overlies Marraba Volcanics, Tewinga Group; conformably overlain by Corella Formation, Overhang Jaspilite. Is correlated with Ballara Quartzite, Double Crossing Metamorphics.|Thick quartzite- and sandstone-dominated unit; contains minor metabasalt and felsic porphyry.|04-APR-17
25245|Mitakoodi Quartzite|65755|6|Mentioned|p3 Fig.1|||Presented in figure legend as Ballara-Mitakoodi Quartzite||||||
25245|Mitakoodi Quartzite|66913|5|Briefly described|p170 fig 1, p172|||Thickness variations in this unit have been attributed to the presence of growth faults which demonstrate continued extension during sedimentation (Potma and Betts, 2006).|1700-1725 Ma|||Younger than Marraba Volcanics.|Arkose, siltstone, basalt, conglomerate, and rhyolitic lenses.|
25245|Mitakoodi Quartzite|67323|4|Described|GIS attrib tbl, p16-17, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mitakoodi Domain, Mount Isa Inlier, Leichhardt Superbasin. A thick quartzose to feldspathic sandstone succession. Occurs as enclaves and screens within Levian Granite.|1755 +/- 4 Ma (Neumann and Fraser, 2007).|Malbon Group.||Overlies Marraba Volcanics. Is overlain by Overhang Jaspilite. Probably equates (at least partly) with Ballara Quartzite. Correlates with lower Quilalar Formation. See COMMENTS.|Quartzite, feldspathic quartzite, siltstone, basalt, schist, minor limestone.|
25245|Mitakoodi Quartzite|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Eastern Succession. Shallow water.||||Overlies Marraba Volcanics, intruded by Wonga Granite, Burstal Granites. Part equivalent to Corella and Quilalar Formations.|Quartzite and sandstones.|
25245|Mitakoodi Quartzite|68542|6|Mentioned|p16 fig 4|||||||||
25245|Mitakoodi Quartzite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with Marraba Volcanics under the symbol, -Pn.||||||
25245|Mitakoodi Quartzite|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
25245|Mitakoodi Quartzite|68732|5|Briefly described|p165-167, p171|Statherian|Statherian|Of the Quilalar Supersequence. Of the Big Supersequence. Sedimentary depositional ages.|1755 +/- 4, 1755 +/- 7, 1756 +/- 3 Ma|||||
25245|Mitakoodi Quartzite|69056|5|Briefly described|p4, p6, p13, p53, Time-Space plot sheet|Statherian|Statherian|Mitakoodi Domain. Combined with other units to form the Mitakoodi Formation, a regionally discrete unit for modelling purposes. Appears as Mitakoodin Quartzite on p4 and p6. Depositional age from rhyolite.|1755 +/- 4 Ma (Neumann and Fraser, 2007).|||Overlies Marraba Volcanics. Equivalent to Ballara Quartzite.||
25245|Mitakoodi Quartzite|69222|5|Briefly described|p222 Fig.2, p223|Statherian|Statherian|Eastern Fold Belt. Associated with the Myally Rift Event.||||Overlies Marraba Volcanics, overlain by Ballara Quartzite||09-FEB-18
25245|Mitakoodi Quartzite|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Is overlain by Overhang Jaspilite.||25-JAN-19
25245|Mitakoodi Quartzite|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone|
25245|Mitakoodi Quartzite|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone|
25245|Mitakoodi Quartzite|69591|4|Described|p29, p33, p35, p50 Fig.2.42, p57, p105|Paleoproterozoic|Paleoproterozoic|Williams (1989). Mitakoodi Domain, Leichhardt Superbasin, Mount Isa Province. Part of Myally Supesequence. Shelf-fluvial deposits. Age based on detrital zircons and rhyolite volcanics (OZCHRON data: Neumann and Fraser, 2007). Partly age-equivalent to Ballara Quartzite.|1755 +/- 7 Ma (Geoscience Asutralia, unpub. data).|Malbon Group.|Wakeful Metabasalt Member.|Overlies Marraba Volcanics. Is overlain by Overhang Jaspilite.|A thick quartzose to feldspathic sandstone succession; siltstone; minor rhyolite volcanics and thin intervals of basaltic lava; schist; minor limestone.|
25245|Mitakoodi Quartzite|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group.|||Quartzose to feldspathic sandstone, siltstone, basalt and mica schist.|
25245|Mitakoodi Quartzite|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group.|||Quartzose to feldspathic sandstone, siltstone, basalt and mica schist.|
25245|Mitakoodi Quartzite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Six un-named sub-units are mapped separately.||Malbon Group.|Wakeful Metabasalt Member.|Overlies Marraba Volcanics.|Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone.|
25245|Mitakoodi Quartzite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Six un-named sub-units are mapped separately.||Malbon Group.|Wakeful Metabasalt Member.|Overlies Marraba Volcanics.|Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone.|
25245|Mitakoodi Quartzite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Malbon Group.||Is overlain by Overhang Jaspilite.|Quartzose to feldspathic sandstone.|
25245|Mitakoodi Quartzite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Quartzose to feldspathic sandstone.|
25245|Mitakoodi Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1730+/-22 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite, conglomerate.|
25245|Mitakoodi Quartzite|71799|4|Described|p150 fig 2, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca. 1750 Ma||Includes the Wakeful Metabasalt Member.|Overlies the Marraba Volcanics. Overlain by the Overhang Jaspilite.|Quartzite.|03-OCT-18
25245|Mitakoodi Quartzite|72596|6|Mentioned|p24|Statherian|Statherian|Geochronologic constraint from a rhyolite within the unit, see Geoscience Australia, 2011: Sample ID 95208070.|1756 +/- 3 Ma||||Includes rhyolite.|
25245|Mitakoodi Quartzite|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Includes 6 informal lithological divisions and one named member within unit. Appears as roof pendants in Wimberu Granite.||Malbon Group|Includes Wakeful Metabasalt Member.|Probably intruded by Wimberu Granite.|Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone. Slate and phyllite, feldspathic to quartzose sandstone, conglomerate and tuff, metabasalt and local porphyritic rhyolite.|
25245|Mitakoodi Quartzite|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Includes 6 informal lithological divisions and one named member within unit. Appears as roof pendants in Wimberu Granite.||Malbon Group|Includes Wakeful Metabasalt Member.|Probably intruded by Wimberu Granite.|Quartzose to feldspathic sandstone, siltstone, basalt and mica schist; minor limestone. Slate and phyllite, feldspathic to quartzose sandstone, conglomerate and tuff, metabasalt and local porphyritic rhyolite.|
25245|Mitakoodi Quartzite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Includes 7 informal lithological divisions within unit.||Malbon Group||Overlying Timberloo Member and Marraba Volcanics. Underlying Overhang Jaspilite.|Siltstone, slate and phyllite. Metabasalt grading into amphibolite and biotite schist, some metasiltstone. Pink feldspathic sandstone and subordinate quartzose sandstone, minor siltstone.|
25245|Mitakoodi Quartzite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Includes 7 informal lithological divisions within unit.||Malbon Group|Includes Wakeful Metabasalt Member.|Overlying Timberoo Member and Marraba Volcanics. Underlying Overhang Jaspilite.|Siltstone, slate and phyllite. Metabasalt grading into amphibolite and biotite schist, some metasiltstone. Pink feldspathic sandstone and subordinate quartzose sandstone, minor siltstone.|
25245|Mitakoodi Quartzite|72889|6|Mentioned|p6 Fig.i.|||||||||
25245|Mitakoodi Quartzite|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
25245|Mitakoodi Quartzite|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
25245|Mitakoodi Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mitakoodi-Tommy Creek Domain.|1755+/-4 Ma crystallisation age of volcanic rocks||||Siliciclastics, minor mafic extrusives.|
25245|Mitakoodi Quartzite|73529|6|Mentioned|p6 Fig.3||||||||Metasedimentary unit.|
26744|Moah Creek beds|22620|6|Mentioned|p188|||||||||
26744|Moah Creek beds|23037|6|Mentioned|p58,70||Permian|Correlates to Back Creek Group and Boomer Formation.||||||
26744|Moah Creek beds|23042|5|Briefly described|p58||Permian|||||||
26744|Moah Creek beds|24076|5|Briefly described|p397 Fig. 2|Late Permian|Late Permian|Max. thickness: 2135m.  Geological Province: Yarrol Basin.||||||
26744|Moah Creek beds|24491|5|Briefly described|p14|Late Permian|Late Permian|||||||
26744|Moah Creek beds|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pm].  Mudstone, lithic sandstone, conglomeratic mudstone, conglomerate.||||||
26744|Moah Creek beds|39252|5|Briefly described|p21|||||||||
26744|Moah Creek beds|41246|6|Mentioned|Map legend|Permian||||||||
26744|Moah Creek beds|41922|4|Described|Table 1, P10|||||||||
26744|Moah Creek beds|43017|6|Mentioned|p377|||||||||
26744|Moah Creek beds|50209|5|Briefly described|Map Legend|Permian|Permian|||||||17-MAY-04
26744|Moah Creek beds|50213|5|Briefly described|Map legend|Permian|Permian|Of the Back Creek Group.  Mudstone, lithic sandstone, conglomeratic mudstone, conglomerate.  Overlie Rookwood Volcanics.||||||17-MAY-04
26744|Moah Creek beds|50317|5|Briefly described|Map Legend|Permian|Permian|Of the Back Creek Group.  Mudstone, lithic sandstone conglomeratic mudstone, conglomerate.||||||09-JUN-04
26744|Moah Creek beds|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Gyranda Subgroup (Back Creek Group).||||||30-JUN-04
26744|Moah Creek beds|60557|5|Briefly described|p19 Fig. 5b, p25|Middle Permian|Middle Permian|Of the Back Creek Group.  Mudstone dominated unit. Unconformably overlie the Rookwood Volcanics; overlain by Dinner Creek Conglomerate. Geological Province: Bowen Basin.||||||09-JUN-05
26744|Moah Creek beds|63773|6|Mentioned|p1059, p1069|||Geological Province: Bowen Basin.||||||07-APR-09
26744|Moah Creek beds|65388|6|Mentioned|p169, 170, 174 Fig 65, p177 Fig 67, p439|Permian|Permian|Grantleigh Subprovince? Compared with conglomerates in Barfield Formation and undivided Back Creek Group. Probably correlative.||||||
26744|Moah Creek beds|68008|3|Fully described|p2, p157, p176-181, p257, p261, p292|Permian|Permian|See also p483, p491. Kirkegaard et al. (1970), named after Moah Creek. The type section is from the head of Emu Creek to its junction with the Fitzroy River, thence W along the river. Age-equivalent to Warminster Formation. Nine facies distinguished. Thickness from >1500m to ~2100m. Sparsely fossiliferous in upper part. Deposition during a brief sag phase.||||Unconformably overlies Rookwood Volcanics. Is overlain by Dinner Creek Conglomerate, and unconformably by Mount Salmon Volcanics. Probable correlative of Back Creek Group and Boomer Formation.|Conglomeratic mudstone and mudstone, with minor conglomerate, coarse-grained lithic sandstone, fine- to medium-grained sandstone. Lithology detailed.|
26744|Moah Creek beds|68679|5|Briefly described|p337-338, p344-346|Permian|Permian|Kirkegaard et al. (1970). Grantleigh Subprovince. Represents a brief sag phase. Sediment sources include the Rockhampton Group and Lorray Formation. Lithologies and fossils described in some detail. Age is early late Permian.||||Unconformably overlies Rookwood Volcanics. Is overlain by the Dinner Creek Conglomerate. Equivalent to Back Creek Group and probably the Boomer Formation.|Conglomeratic mudstone in the lower part; the upper part of massive mudstone has two facies associations: (A) has fine-grained clastics: sandstone beds and interbedded siltstones; (B) has conglomerate, diamictite and sandstone.|
39065|Molangul Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
39065|Molangul Granite|67203|6|Mentioned|p6|Triassic|Triassic|||||||
39065|Molangul Granite|68008|3|Fully described|p326, p329, p332, p414-416|||Dear et al. (1971). Named after Mount Molangul; the type section is on its southern flanks. Forms rugged, mountainous country 18km long. Geophysics briefly described. Geochemistry described: contains alkali amphiboles; within-plate granite field. Not isotopically dated; thought to be Late Triassic because of similarities with other local granites of that age, but it also resembles the mid-Permian Castletower Granite.||||Intrudes Wandilla Formation.|Pale to dark pink, fine- to medium-grained, slightly porphyritic, leucocratic amphibole-bearing syenogranite; almost invariably slightly to moderately altered. An A-type, alkaline to peralkaline, subsolvus granite.|
39065|Molangul Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pink, medium-grained, equigranular, hornblende syenogranite with common rounded, fine-grained granite and microgranite inclusions.|
39065|Molangul Granite|68679|5|Briefly described|p428, p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region, northern New England Orogen. Mapped as one unit with Bulburin Granite on p428.|||||Pink, medium-grained, equigranular, hornblende syenogranite with common rounded, fine-grained granite and microgranite inclusions; granophyric, miarolitic cavities; arfvedsonite(?); pegmatite patches. A-type; alkaline to peralkaline.|
39065|Molangul Granite|73450|4|Described|p8, p10, p15-21, p23, p28, p35, p37|late Triassic|late Triassic|A-type. Previously mapped mainly as Muncon Volcanics and partly as Miriam Vale Granodiorite (Ellis, 1974). Irregular-shaped pluton northeast of Monto. Forms rugged, inaccessible, mountainous country. Irregular miarolitic cavities (up to ca 1 cm across) are common. Not yet radioisotopically dated although it is most probably late Triassic. Interpreted to post-date the adjacent Bootoo Creek Granite, Bulburin Granite, Gaeta Diorite, and Bobby Volcanics. It is cut by very few dykes, if any.||||Intrudes Wandilla Formation, Shoalwater Formation, Cassilis Granite, and Glen Eva Complex.|Pale to dark pink, fine- to medium-grained, uneven grained to slightly porphyritic, amphibole-bearing syenogranite; almost invariably slightly to moderately altered.|
26746|Molloy beds|23422|5|Briefly described|Plate 7.3|Early Carboniferous|Late Silurian|||||||
26746|Molloy beds|23423|4|Described|p301 Table 7.2|Carboniferous|Late Devonian|Contains a number of graded beds and sedimentary cycles. Also see p233-234, p290.  Hodgkinson Province.||||||
26746|Molloy beds|23430|4|Described|p511|||Also see p471. Hodgkinson Province.||||||
26746|Molloy beds|42658|3|Fully described|p25|Carboniferous?||Reserved as Molloy Beds.||||||
26746|Molloy beds|43285|5|Briefly described|Map Legend|||age Late Devonian? to Carboniferous?||||||
26746|Molloy beds|43625|4|Described|p19,26,31|||||||||
26746|Molloy beds|50387|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Arenite, siltstone and mudstone.  Geological Province: Hodgkinson Province.||||||23-JUN-04
26746|Molloy beds|60425|3|Fully described|p13, p16 Tb. 1, p28|Early Carboniferous|Late Devonian|Faulted against Hodgkinson Formation. Age is inferred. Max. thickness: >235m. Geological province: Hodgkinson Province. Rhythmically interbedded, arenite, siltstone, mudstone; no fossils.||||||07-FEB-11
26746|Molloy beds|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.||||||
26746|Molloy beds|69592|5|Briefly described|p232, p238|||Cranfield and Hegarty (1989). Forms a small (~5km) belt south of Mount Molloy in central Palmer-Barron Subprovince. Previously mapped (deKeyser and Lucas, 1968; Gregory, 1977) as part of Hodgkinson Formation. Probably obsolete, or as the authors describe it, "unsustainable", and is now regarded as part of the Hodgkinson Formation again.|||||Thin- to medium-bedded sandstone and mudstone.|
22359|Molly Darling Granodiorite|22847|3|Fully described|p 53|Early Devonian|Late Silurian|||||||
22359|Molly Darling Granodiorite|23422|5|Briefly described|p191, p213 Table 6.8|||||||||
22359|Molly Darling Granodiorite|23430|5|Briefly described|p486|||||||||
22359|Molly Darling Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22359|Molly Darling Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 497. I-Type.||||||
22359|Molly Darling Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
22359|Molly Darling Granodiorite|43259|4|Described|Appendix 1,p52.|Early Devonian|Late Silurian|||||||
22359|Molly Darling Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22359|Molly Darling Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Molly Darling gdrt.||Unit in Millchester Supersuite.||||
22359|Molly Darling Granodiorite|64852|5|Briefly described|Map legend|Devonian|Silurian|Altered, medium-grained, porphyritic, hornblende-biotite granodiorite and tonalite.||||||
22359|Molly Darling Granodiorite|68900|6|Mentioned|p4, p39|Middle Devonian|Silurian|Drummond Basin.||||||
80776|Molongle Creek Granite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Pale pinkish grey to pale pink, medium-grained, even-grained biotite monzogranite to hornblende-biotite granodiorite(?); deeply weathered and poorly exposed; cut by mafic and felsic dyke.|
22360|Molybdenite Creek Granite|22847|3|Fully described|p 57|Permian|Carboniferous|||||||
22360|Molybdenite Creek Granite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
22360|Molybdenite Creek Granite|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22360|Molybdenite Creek Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 181. I-Type.||||||
22360|Molybdenite Creek Granite|43093|4|Described|Appendix 1|Permian|Carboniferous|||||||
22360|Molybdenite Creek Granite|43259|4|Described|Appendix 1,p28.|Permian|Carboniferous|||||||
22360|Molybdenite Creek Granite|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22360|Molybdenite Creek Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Suite.||||
41324|Monaghans Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1804Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
41324|Monaghans Granite|50100|5|Briefly described|p13 Fig.4|Orosirian|Orosirian|Geological Province: Western Fold Belt Province.||||||
41324|Monaghans Granite|50536|5|Briefly described|p1.5, 11.3, Table 1.1|||Geological Province: Mount Isa Inlier. Of the Monaghans Suite.||||||
41324|Monaghans Granite|67323|4|Described|GIS attrib tbl, p10, p23|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. See also references to Moonaghans Granite (p6-7). Ardmore-May Downs Domain, Mount Isa Inlier. Post-Barramundi Orogeny: Big Toby Igneous Event (intraplate magmatism). Intrusions 1820-1800 Ma.|1804 +/- 6 Ma.|Big Toby Suite.||Age correlation with Big Toby and Yeldham Granites.|Biotite tonalite to monzogranite|
41324|Monaghans Granite|69591|4|Described|p30, p32, p60|||Ardmore-May Downs Domain, Mount Isa Province. An age of 1804 +/- 15 Ma by Page and Sun (1998) is also given.|1805 +/- 15 Ma (Wyborn et al., 1988).|Big Toby Suite.||Intrudes Yaringa Metamorphics.|Biotite tonalite to monzogranite.|
41324|Monaghans Granite|71592|5|Briefly described|Appendix A.|||Mount Oxide Domain, Mount Isa Orogen.|1804+/-15 Ma (crystallisation: U-Pb zircon TIMS).||||Granite.|
41324|Monaghans Granite|73525|5|Briefly described|p4-5 Fig.2, p17, p19 Fig.13|Statherian|Orosirian|Leichhardt River Domain.|1804+/-6 Ma crystallisation age||||Felsic intrusive.|
41324|Monaghans Granite|73553|6|Mentioned|p259|Statherian|Orosirian|Western Fold Belt.|1805+/-15 Ma (Wyborn et al., 1988)|||||
38874|Monal Granodiorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
38874|Monal Granodiorite|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38874|Monal Granodiorite|24615|5|Briefly described|CD|Triassic|Triassic|[Rggm/d].  Grey medium-grained biotite-hornblende granodiorite to quartz diorite.||||||
38874|Monal Granodiorite|68008|2|Defined|p213, p334, p338, p397-401, p403, p444|Triassic|Triassic|See also p451, p460, p635. Western end of Glassford Igneous Complex. Forms an elongate, ENE-trending intrusion, 15 x 2 km, 35km N of Monto. Named after Monal Creek. The type area extends from Spring Creek to Broad Creek, and is centred on Monal Creek. Varied topography described. Geophysics described in some detail and modelled; contrasted with other units in the Igneous Complex. Geochemistry detailed. No age determination; considered Triassic because of close relationship with Littlemore Granodiorite. Abuts Littlemore Granodiorite. Hosts the Monal Goldfield.||Glassford Igneous Complex.||Intrudes Three Moon Conglomerate. Is intruded by Burns Spur Nepheline Monzonite, Ridler Monzonite, and Dooloo Tops Volcanics. Is overlain nonconformably by Dooloo Tops Volcanics.|Two phases. 1: grey, medium-grained, equigranular biotite-hornblende granodiorite to tonalite; local biotite-hornblende quartz diorite. 2: medium-grained, grey biotite-hornblende granodiorite to pink hornblende-biotite granite. Rhyolite dyke swarms.|
38874|Monal Granodiorite|68679|5|Briefly described|p427, p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Geochemistry briefly described.||Glassford Igneous Complex.||Adjacent to Ridler Monzonite. Is overlain by Dooloo Tops Volcanics.|Mafic rim of grey, medium-grained biotite-hornblende granodiorite to quartz diorite, some hornfelsing and shear zones; pale grey to pink, medium-grained hornblende-biotite granodiorite and granite intrudes the marginal phase.|
38874|Monal Granodiorite|69594|5|Briefly described|p561|Triassic|Triassic|||||Is intruded by Burns Spur Nepheline Monzosyenite, Ridler Monzonite and Glassford Igneous Complex.||
38874|Monal Granodiorite|73450|6|Mentioned|p11, p59, p65|Triassic|Triassic|||||Intruded by Ridler Monzonite and Burns Spur Nepheline Monzosyenite (Glassford Igenous Complex).||
39550|Monal Suite|23799|5|Briefly described|p115 Fig. 10, p117|||Geological Province: Yarrol Province.||||||
70384|Monduran Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian|The 2 facies are mapped separately.|||||Pale pink, medium to coarse-grained, porphyritic biotite monzogranite; fine-grained granodiorite or diorite?|
32155|Monkey Springs Granite|23037|5|Briefly described|p81|Permian|Silesian|||||||
32155|Monkey Springs Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Cgmy].  Red to orange, medium-grained granite to leucogranite.||||||
32155|Monkey Springs Granite|50273|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Red to orange, medium-grained granite to leucogranite.||||||
32155|Monkey Springs Granite|65388|2|Defined|p265-266, p236 Fig. 81, p237, 238|Late Carboniferous|Late Carboniferous|Relationship with surrounding Torsdale Volcanics is unclear. Possibly co-magmatic. Pink to red, medium-grained fractionated granite.||||||
32155|Monkey Springs Granite|68679|5|Briefly described|p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.|||||Pink to red, medium-grained fractionated granite.|
75606|Monte Christo Granite|69594|5|Briefly described|p567 Fig.7.39|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.||||||
24385|Monte Christo Member|39493|2|Defined|p99|late Eocene|middle Eocene|Mid to Late Eocene||||||
24385|Monte Christo Member|39997|6|Mentioned|p165|||||||||
24385|Monte Christo Member|40116|6|Mentioned|Fig.4|||||||||
24385|Monte Christo Member|41927|5|Briefly described|p64|||||||||
24385|Monte Christo Member|42021|6|Mentioned|Fig.3 P320|||||||||
24385|Monte Christo Member|71092|6|Mentioned|p232|Eocene|Eocene|||Rundle Formation.||||
29606|Monto Basalts|43005|6|Mentioned|Fig.1 p214|||||||||
32131|Montour Gabbro|23037|4|Described|p82,4,5||Early Permian|||||||
32131|Montour Gabbro|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgmt].  Dark green to dark grey, fine to medium-grained gabbro.||||||
32131|Montour Gabbro|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
32131|Montour Gabbro|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Dark green to dark grey, fine- to medium-grained gabbro.||||||
32131|Montour Gabbro|65388|3|Fully described|p266-267, p236, p237, 238, 248, 271|Early Triassic|Permian|Dark green and white, medium-grained gabbro. Appears to have been intruded late in the magmatic cycle forming discrete bodies within different granitoid plutons (Pinedale Granite). Could be early Permian, related to basalts in the Camboon Volcanics, or part of the late Permian to Early Triassic suite of gabbros. Interpreted as older than Dawson Granite.||||||
32131|Montour Gabbro|68679|5|Briefly described|p407-408|Permian|Permian|Auburn Subprovince, New England Orogen. Comprises three bodies in a WNW line. May have intruded late in the magmatic cycle; could be early Permian or late Permian-Middle Triassic.||||Intrudes Keen Creek Granite. Is intruded by Pinedale Granite.|Dark green and white, medium-grained gabbro; dark green fine-grained gabbro; greenish-grey, medium-grained layered leucogabbro.|
83308|Monument Syenite|73413|6|Mentioned|p5-6, p9, p12, p15, p23|Calymmian|Calymmian|[Also written as Monument syenite]. Syn-tectonic emplacement[?]. An imprecise K-Ar biotite age of ca. 1420 MA was reported by Richards et al. (1963).|ca. 1420 Ma|||||
39148|Moocoorooba Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgmo].  Pale grey to pink, medium-grained hornblende-biotite granite to granodiorite.||||||
39148|Moocoorooba Granite|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
39148|Moocoorooba Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pale grey to pink, medium-grained, hornblende-biotite granite to granodiorite.||||||
39148|Moocoorooba Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
39148|Moocoorooba Granite|61087|5|Briefly described|Map Legend|Permian|Carboniferous|Buff to dark pink, or pale grey, medium to coarse-grained, even-grained to moderatly porphyritic, hornblende-biotite and biotite granite; some diorite and leucogranite.||||||
39148|Moocoorooba Granite|65388|1|Redefined|p267, p236, 237, 238, 247, 262, 303,304|Carboniferous|Carboniferous|Replaces Moocoorooba Adamellite. Probably intruded by the Glencoe Gabbro. May have been intruded by, or be related to Crystal Vale Monzogranite. Interpreted to post-date J P Granite. Mapped in contact with numerous other granitoid and gabbro units, most of which are probably Carboniferous. The relationship to these is uncertain.  Late Carboniferous age likely. Pale to moderate pink medium-grained equigranular (hornblende)-biotite granite.||||||
39148|Moocoorooba Granite|68679|5|Briefly described|p404, p408|Late Carboniferous|Late Carboniferous|Auburn Subprovince, New England Orogen. Age uncertain.||||Probably intruded by Glencoe Gabbro.|Pale to moderate pink, medium-grained, equigranular (hornblende-)biotite granite with a weak foliation.|
23804|Moolboolaman Granodiorite|24382|5|Briefly described|Map legend|Triassic|Permian|||||||
23804|Moolboolaman Granodiorite|39505|6|Mentioned|p191|||||||||
23804|Moolboolaman Granodiorite|39997|6|Mentioned|p165|||||||||
23804|Moolboolaman Granodiorite|41778|2|Defined|Table 2|Triassic|Permian|||||||
23804|Moolboolaman Granodiorite|42054|6|Mentioned|p273|||||||||
23804|Moolboolaman Granodiorite|63821|5|Briefly described|p29|Triassic|Permian|Intrudes Curtis Island Group and Good Night beds; intruded by Hogback Granite. Porphyritic biotite-hornblende granodiorite and biotite-hornblende granite||||||07-FEB-11
23804|Moolboolaman Granodiorite|64556|5|Briefly described|p51-55, p56|||Concordia age of magmatic emplacement: 224.0+/-1.2Ma. Age analysis details included. Sample analysed is from massive equigranular biotite-hornblende granodiorite.||||||07-FEB-11
23804|Moolboolaman Granodiorite|65452|5|Briefly described|p7 Tb.2|Late Triassic|Late Triassic|SHRIMP U-Pb zircon magmatic crystallisation age.|224 +/- 1.2 Ma (Carson et al. 2006).||||Massive, equigranular, hornblende-biotite granodiorite.|
23804|Moolboolaman Granodiorite|67203|5|Briefly described|p3-4|Triassic|Triassic||224 +/- 1.2 Ma (Carson et al., 2006).||||Massive, equigranular, hornblende-biotite granodiorite.|
23804|Moolboolaman Granodiorite|68421|5|Briefly described|Map Legend|Norian|Norian|Triassic Igneous Province. Age determined from a site on the Mount Perry sheet area.|224.0 +/- 1.2 Ma||||Biotite-hornblende granodiorite, diorite, pyroxene-hornblende tonalite, pyroxene-hornblende granite.|12-NOV-15
23804|Moolboolaman Granodiorite|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. A small, elongate intrusion.|224.0 +/- 1.3 Ma (SHRIMP: Carson et al., 2006).|||Adjacent to Wonbah Granodiorite.|Mainly massive, equigranular, locally porphyritic, biotite-hornblende granodiorite to tonalite and biotite granite, with locally abundant microdiorite and metasedimentary enclaves.|
23804|Moolboolaman Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|224+/-1.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
23804|Moolboolaman Granodiorite|73450|6|Mentioned|p24|||||||Intruded by Hogback Granite.||
39134|Moolyung Granodiorite|64556|5|Briefly described|p48-51, p56|Late Triassic|Late Triassic|Age of crystallisation: 227.5+/-1.5Ma. Age analysis details included. Sample analysed is from massive equigranular hornblende-titanite granodiorite.||||||07-FEB-11
39134|Moolyung Granodiorite|65452|5|Briefly described|p7 Tb.2|Late Triassic|Middle Triassic|A SHRIMP U-Pb zircon age of 225 +/- 2 Ma for the porphyritic and miarolitic Eastern Pluton of this unit was obtained by Black (unpublished).|227.5 +/- 1.5 Ma (Carson et al. 2006).||||Massive hornblende titanite granodiorite; medium-grained, porphyritic, miarolitic, clinopyroxene-biotite-hornblende granodiorite.|
39134|Moolyung Granodiorite|67203|5|Briefly described|p2-4|Late Triassic|Late Triassic|One of several intrusives emplaced around the time of Agnes Water Volcanics. Ages from Carson et al., (2006) and Black (unpublished) respectively.|227.5 +/- 1.5 Ma and 225 +/- 2 Ma.||||Massive, hornblende-titanite granodiorite; medium-grained, porphyritic, miarolitic, clinopyroxene-biotite-hornblende granodiorite.|
39134|Moolyung Granodiorite|68332|5|Briefly described|Map legend.|Late Triassic|Late Triassic|Triassic Igneous Province.|225.0 +/- 2.0 Ma.|||Intrudes Brooweena Formation?.|Pale grey to white, coarse-grained, equigranular hornblende granodiorite with scattered  microdiorite enclaves up to 3 cm across.|20-MAR-15
39134|Moolyung Granodiorite|68421|5|Briefly described|Map Legend|Carnian|Norian|Triassic Igneous Province. Zircon U-Pb age.|227.5 +/- 1.5 Ma (Carson et al., 2006).||||Pale grey to white, coarse-grained, equigranular hornblende granodiorite with scattered microdiorite enclaves up to 3 cm across.|
39134|Moolyung Granodiorite|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Geochemically similar to Wally Creek and Colosseum Quartz Monzodiorites.|227.5 +/- 1.5 Ma (SHRIMP: Carson et al., 2006).||||Mostly pale grey, medium- to coarse-grained, equigranular to slightly porphyritic biotite and hornblende granodiorite to monzodiorite, with some tonalite and granite; may contain abundant mafic inclusions.|
39134|Moolyung Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|228+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
39552|Moonkan Granite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
39552|Moonkan Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbo].  Pale pinkish grey medium-grained biotite-hornblende granite.||||||
39552|Moonkan Granite|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
39552|Moonkan Granite|68008|2|Defined|p248, p333, p341, p346-350, p352, p620|Permian|Permian|Defined in this study. Previously the granodiorite transitional to granite phase of the Westwood Complex of Wood (1974). A small pluton and several small outcrops E of Mount Hay. Named from Moonkan pastoral holding; the type area is in its central part, 3.5km SSE of Wycarbah. Forms prominent rocky, forested hills with large outcrops, tors and boulders. Geochemistry described. Ages by Wood (1974); Ford et al. (1976). Also 243 +/- 2 Ma (corrected) by Webb and McDougall (1968). Geophysics modelling.|257 +/- 5 Ma; 251 +/- 5 Ma (K-Ar biotite).|Bouldercombe Igneous Complex.||Intrudes Umbrella Granodiorite.|Pale pinkish-grey, massive, equigranular, medium-grained hornblende-biotite granite, locally containing sparse fine-grained grey xenoliths. Plagioclase slightly dominates quartz and K-feldspar.|
39552|Moonkan Granite|68679|4|Described|p424, p426-427|||Yarrol Province. A ~3 x 1km unit in the western lobe of the Complex. Geochemistry briefly described. Other ages given.|251 +/- 5 Ma (Ford et al., 1976).|Bouldercombe Igneous Complex.||Intrudes Umbrella Creek Granodiorite.|Biotite-hornblende granite.|
23805|Mooramin Granite|42747|5|Briefly described|p37, p39|||||||||
23805|Mooramin Granite|43029|2|Defined|p14|Late Cambrian|Middle Cambrian|see also Fig.1,p13||||||
23805|Mooramin Granite|43204|5|Briefly described|Map Legend|Ordovician|Cambrian|Anakie Inlier||||||23-DEC-11
23805|Mooramin Granite|43213|3|Fully described|p9, p17, p30, p74, p95, p98-101, p117|||See also p121-124, p220. Fletchers Awl area. Mapped and described by Hayward (1993). Type locality described. Geochemistry detailed. Age unknown. Could be much older than the unrelated Retreat Batholith. Lithology detailed.||||Is overlain unconformably by Greybank Volcanics.|Foliated cordierite-bearing muscovite-biotite granite with abundant schlieren and biotite-schist and quartz xenoliths. S-type.|
23805|Mooramin Granite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
23805|Mooramin Granite|68731|5|Briefly described|p123 Fig 3.10, p130, p131, p132|Late Ordovician|Early Ordovician|Anakie Province. Exhibits weak to very strong subvertical foliation that strikes southeast. Contains abundant country-rock xenoliths. S-type granite.|463 +/- 15 Ma (U-Pb zircon LA-ICP-MS)|||Nonconformably overlain by the Greybank Volcanics.|Cordierite-bearing with abundant biotite-rich schlieren and metasedimentary xenoliths. Includes quartz, plagioclase, K-feldspar, biotite, muscovite, and cordierite pseudomorphed by fine phyllosilicates. Migmatitic phases occur locally.|
23805|Mooramin Granite|68900|6|Mentioned|p4|Ordovician|Ordovician|Drummond Basin.||||||
23805|Mooramin Granite|70744|5|Briefly described|p939|||Anakie Province.|c.480 Ma (estimated from Fig.7).|||||
23805|Mooramin Granite|70749|5|Briefly described|p43|Ordovician|Ordovician|Anakie Province.|463 +/- 15 Ma.|||||
23805|Mooramin Granite|71966|6|Mentioned|p989-990|Middle Ordovician|Middle Ordovician|Geological province: Anakie Province, Thomson Orogen. Magmatism associated with the 490-460 Ma Larapinta extensional event.|463+\-15 Ma|||||
23805|Mooramin Granite|73425|6|Mentioned|p15-16|Early Ordovician|Early Ordovician|Anakie Province, northeast Thomson Orogen.|463 +/- 15 Ma (Richards et al., 2013).|||||
23807|Mooremount Granite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Pinkish grey to grey, medium- to fine-grained (muscovite-) biotite granite.||||||
23807|Mooremount Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
23807|Mooremount Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 807. S-Type.||||||
23807|Mooremount Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
23807|Mooremount Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23807|Mooremount Granite|40659|6|Mentioned|p250|||||||||
23807|Mooremount Granite|40954|6|Mentioned|p133|||||||||
23807|Mooremount Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
23807|Mooremount Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
23807|Mooremount Granite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Pinkish-grey to grey, medium- to fine-grained (muscovite-)biotite granite and apparently slightly younger grey to pinkish-grey (muscovite-)biotite granite with inclusions of the finer-grained granite.|
23807|Mooremount Granite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Pinkish-grey to grey, medium- to fine-grained (muscovite-)biotite granite and apparently slightly younger grey to pinkish-grey (muscovite-)biotite granite with inclusions of the finer-grained granite.|
24386|Moorooloo Mudstone Member|13516|5|Briefly described|p145 fig 3, p146 fig 4, p150|Early Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP3101 - APP3102||Cattle Creek Formation||||
24386|Moorooloo Mudstone Member|37726|2|Defined|p158|Early Permian|Early Permian|||||||
24386|Moorooloo Mudstone Member|38658|6|Mentioned|p152|||||||||
24386|Moorooloo Mudstone Member|39263|6|Mentioned|Fig.2|||||||||
24386|Moorooloo Mudstone Member|39273|6|Mentioned|p305|||||||||
24386|Moorooloo Mudstone Member|39943|6|Mentioned|Table 5A|||||||||
24386|Moorooloo Mudstone Member|41605|6|Mentioned|Fig.2|||||||||
24386|Moorooloo Mudstone Member|43050|5|Briefly described|p6|||of Cattle Creek Formation||||||
24386|Moorooloo Mudstone Member|60286|5|Briefly described|p298 Fig.11|Early Permian|Early Permian|Of Cattle Creek Formation. Overlain by Staircase Sandstone Member. Contains Cruziana trace fossil assemblage. Geological Province: Bowen Basin.||||||
24386|Moorooloo Mudstone Member|68576|5|Briefly described|Q_4: p19|Early Permian|Early Permian|Denison Trough.||Cattle Creek Formation.||||22-OCT-19
23809|Mopata Microgranite|23291|5|Briefly described|p97 Tb. 3.11|Carboniferous|Carboniferous|Of the Newcastle Range I-types. Geological Province: Georgetown Region.||||||08-JUL-15
23809|Mopata Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 47. I-Type.||||||
23809|Mopata Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23809|Mopata Microgranite|40542|6|Mentioned|p97|||||||||
23809|Mopata Microgranite|43259|4|Described|Appendix 1,p18.||Carboniferous|||||||
23809|Mopata Microgranite|43740|4|Described|p17|||||||||
23809|Mopata Microgranite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
23809|Mopata Microgranite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Brown, moderately to abundantly porphyritic biotite and hornblende-biotite microgranite.|
23809|Mopata Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Newcastle Range Volcanic Group.|||||I-type: biotite microgranite and granite.|
41267|Morang Volcanics|50598|5|Briefly described|Map Legend|Triassic|Triassic|Flow banded and autobrecciated trachyte, lithic conglomerate, amygdaloidal andesite.||||||
41267|Morang Volcanics|65388|4|Described|p206, p 204 Fig72, p305, 306, 347|Triassic|Triassic|Described by Whitaker & others (1974) but not named. "Rosehall Volcanics" was used informally by Peko-Wallsend Operations Ltd. Thickness >300m. Probably intruded by Mount Saul Quartz Monzonite.  Age based on lithological correlation.||||||
41267|Morang Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
41267|Morang Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
41267|Morang Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
41267|Morang Volcanics|68679|5|Briefly described|p312-313, p353, p429, p434, p441|Triassic|Triassic|Northern New England Orogen. Is associated with the Rosehall Caldera; is also known "informally" as the Rosehall Volcanics. May have a genetic relationship involving magma mixing with Mount Saul Quartz Monzonite. Both are transitional between I-type and A-type.|215.168 +/- 2.7 Ma (K-Ar whole rock: Morgan, 1993)|||Is partly enclosed by the Mount Saul Quartz Monzonite.|Basal interbedded amygdaloidal, autobrecciated andesite lavas and andesitic ignimbrites overlain (following caldera collapse) by rhyolitic ignimbrites and lava domes with flow-banded cores and autobrecciated margins.|
28001|Morehead Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite.||||||
28001|Morehead Granite|43596|4|Described|p35, p26 Tb. 2, p27 Tb. 3|||Of Ebagoola Suite (Kintore Supersuite). Intrudes Kimba+Penny Gneisses, + Dinah Formation; intruded by Imooya Granite. Sparsely porph.to equigran. muscovite-biotite granite, garnet-muscovite granite+garnet-biotite-muscovite leucogranite; pegmatite; aplite.||||||07-APR-15
28001|Morehead Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
34119|Morepork Member|22630|4|Described|p 18|||||||||
34119|Morepork Member|22844|2|Defined|Fig4 p13,18,19,24|Cambrian|Mesoproterozoic|Within Cape River Metamorphics||||||
34119|Morepork Member|23422|5|Briefly described|p167|||Of Cape River Metamorphics.||||||
34119|Morepork Member|23499|5|Briefly described|map legend|Cambrian|Neoproterozoic|Of Cape River Metamorphics. Age: Neoproterozoic or Cambrian.||||||
34119|Morepork Member|23508|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|of Cape River Metamorphics.||||||
34119|Morepork Member|61211|5|Briefly described|p263|||Of the Cape River Metamorphics. Has white quartzite ridge-forming horizons interlayered with mainly metasandstone and minor graphiticschist. ||||||
34119|Morepork Member|68731|5|Briefly described|p137, p137 Fig 3.22, p139, p141|Cambrian|Neoproterozoic|Contains numerous white ridge-forming quartzites, usually in 50-100 m thick bands, with metasandstone and mica schist. Age constrained by the Cape River Metamorphics.||Of the Cape River Metamorphics.||||
75761|Morer Granite|70740|5|Briefly described|p127|||Outcrop characteristics and distribution briefly discussed. ||||Intrudes the Seventy Mile Range Group.|Fine to medium-grained, porphyritic hornblende-biotite monzogranite with traces of allanite, sphene and numerous mafic inclusions.|
26043|Morney profile|35793|2|Defined|p243|early Eocene|Maastrichtian|Maastrichtian to Early Eocene.||||||
26043|Morney profile|66623|5|Briefly described|p270.|Paleocene|Late Cretaceous|Weathering event which resulted in kaolinisation of Cretaceous sedimentary rocks to depths over 100 m in southwest Queensland. Clasts occur in Eyre Formation. Where it was not subsequently covered, it was truncated and silicified to form silcrete.||||||
26043|Morney profile|69599|5|Briefly described|p581, p599, p601, p649-650|Paleocene|Late Cretaceous|Southwest QLD; may extend into the Gulf of Carpentaria. ~95m thick. Required at least 100,000 years to develop. Appears as Morney Profile on p649.||||Is overlain by Curalle silcrete (profile).|Kaolinised, ferruginised, mottled and silicified surface.|
26043|Morney profile|70821|6|Mentioned|p24|||Senior and Mabbutt (1979). A prominent weathering profile used for correlation across the Eromanga Basin, a practice disputed and avoided in this study.||||||
80679|Morris Granite|71849|4|Described|p4, p8, p17, p33-46, p134, p141, p149|Devonian|Devonian|See also p151, p162-168, p170, p176, p195. NNE-aligned pluton of ~115km2, W of Archer River Shear Zone, Coen area. Included in Blue Mountains Supersuite by Knutson et al. (1994). Previously the main component of the Morris Adamellite of Willmott et al. (1973) and Whitaker and Gibson (1977). Crops out as massive boulders, pavements in watercourses, and low bouldery hills. Described in detail. Photomicrographs.|407 +/- 8 Ma (SHRIMP U-Pb; Black et al., 1992).|Blue Mountains Supersuite.||Intrudes Yarraden Schist. Is intruded by Wolverton Granite. Is overlain nonconformably by Gilbert River Formation.|Mainly pale grey, medium-grained, highly porphyritic biotite monzogranite, with prominent large K-feldspar phenocrysts.|
80679|Morris Granite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Blue Mountains Supersuite.|||Mainly pale-grey, medium-grained, highly porphyritic biotite monzogranite, with prominent large K-feldspar phenocrysts.|
80679|Morris Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Blue Mountains Supersuite.|||Mainly pale grey, medium-grained, highly porphyritic biotite monzogranite, with prominent large K-feldspar phenocrysts.|
80679|Morris Granite|73387|6|Mentioned|p1, p29|Early Devonian|Early Devonian|Magmatic crystallisation age of 407 +/- 8 Ma from Black et al. (1992).|407 +/- 8 Ma SHRIMP zircon|Blue Mountains Supersuite||||20-DEC-22
69003|Morrow Granite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Strongly altered leucogranite.||||||
69003|Morrow Granite|65388|3|Fully described|p326-328, p236, 301, 303, 304, 340|Triassic|Late Permian|New unit. Of Tandora Suite. Adjacent to Donore Granite Gneiss. Distinguished on magnetic response. Outcrop very poor. Late Triassic Boolgal Granite appears to intrude. Age not known. Likely age range given. Cream, strongly decomposed, fine-grained equigranular granite containing strongly leached biotite.||||||
69003|Morrow Granite|68679|5|Briefly described|p419|||Rawbelle Batholith, northern New England Orogen. ~70 km2.||Tandora Suite.||Intruded by dykes of ?Mount Eagle Volcanics or ?Boolgal Granophyre.|Strongly altered leucogranite; cut by abundant rhyolite dykes.|
69003|Morrow Granite|73450|6|Mentioned|p28|||Rawbelle Batholith.||||Intruded by Boolgal Granophyre.||
35187|Morugo Granite|23042|4|Described|p91,2,3, Fig 2||Early Cretaceous|Intrudes Palms Lookout Granite.||||||
35187|Morugo Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35187|Morugo Granite|61917|5|Briefly described|Map legend|Cretaceous|Cretaceous|Light grey, coarse-grained biotite granite and grey, fine- to medium-grained hornblende-biotite granodiorite; quartz diorite and layered, fine- to medium-grained hornblende gabbro; porphyritic microgranite, andesite and rhyolite dykes.||||||
35187|Morugo Granite|65388|2|Defined|p408-410, p135, 362, 364, 365, 378, 379|Early Cretaceous|Early Cretaceous|Southern Urannah Batholith? Probably intrudes Palms Lookout Granodiorite, Uruba Granite. K-Ar crystallisation ages: 130+/-1 Ma and 129+/-1 Ma from biotite and hornblende respectively (Webb & McDougall, 1964). Mainly fine to medium-grained, equigranular hornblende-biotite granite or granodiorite. Very poorly exposed. See also p 389, 395.||||||
35187|Morugo Granite|69594|5|Briefly described|p565-566|Early Cretaceous|Early Cretaceous|Urannah Batholith.|130 +/- 1 Ma (K-Ar: Webb and McDougall, 1964).||||Locally foliated to gneissic.|
35187|Morugo Granite|73037|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Light grey, coarse-grained biotite granite and grey, fine to medium-grained hornblende-biotite granodiorite; quartz diorite and layered, fine to medium-grained hornblende gabbro; porphyritic microgranite, andesite and rhyolite dykes.|
27497|Mosaic Gully Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Age: 325+/-5Ma. Thickness: Up to 1000m. Geological Province: Georgetown Region.||||||08-JUL-15
27497|Mosaic Gully Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V25. Assumed to be I-Type.||||||
27497|Mosaic Gully Rhyolite|23619|4|Described|p31 Table 1||Carboniferous|Intruded by Caterpillar Microgranite. Of Eveleigh Volcanic Subgroup, of Newcastle Range Volcanic Group. Overlying Unit Shrimp Creek Rhyolite. Underlying Unit Beril Peak Rhyolite.||||||28-MAY-15
27497|Mosaic Gully Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27497|Mosaic Gully Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
27497|Mosaic Gully Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Eveleigh Volcanic Subgroup||||||
27497|Mosaic Gully Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
27497|Mosaic Gully Rhyolite|43740|5|Briefly described|p13|||||||||
27497|Mosaic Gully Rhyolite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Of the Newcastle Range Volcanic Group).||||||
27497|Mosaic Gully Rhyolite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Ignimbrite. Of the Eveleigh Volcanic Subgroup.||||||19-AUG-04
27497|Mosaic Gully Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|||Brown, crystal-poor to crystal-rich rhyolitic ignimbrite, locally containing sparse chlorite; buff to purple, crystal-rich rhyolitic ignimbrite (25% quartz and feldspar crystals).|
27497|Mosaic Gully Rhyolite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|The 2 facies are mapped separately. Kennedy Province.||Of the Eveleigh Volcanic Subgroup.|||Buff to purple, crystal-rich rhyolitic ignimbrite (25% quartz and feldspar crystals); brown crystal-poor to crystal-rich rhyolitic ignimbrite, locally containing sparse chlorite.|
27497|Mosaic Gully Rhyolite|69593|5|Briefly described|p512|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|330 Ma.|Newcastle Range Volcaniuc Group.|||I-type.|
24387|Mostyndale Mudstone Member|13516|5|Briefly described|p145 fig 3, p146 fig 4, p150|Early Permian|Early Permian|From Denison Trough, Bowen Basin.  Age APP222 - APP3101||Cattle Creek Formation||||
24387|Mostyndale Mudstone Member|37726|2|Defined|p155|Early Permian|Early Permian|||||||
24387|Mostyndale Mudstone Member|38658|6|Mentioned|p152|||||||||
24387|Mostyndale Mudstone Member|39273|6|Mentioned|p305|||||||||
24387|Mostyndale Mudstone Member|39943|6|Mentioned|Table 5B|||||||||
24387|Mostyndale Mudstone Member|41514|6|Mentioned|p82|||||||||
24387|Mostyndale Mudstone Member|41605|6|Mentioned|Fig.2|||||||||
24387|Mostyndale Mudstone Member|43050|5|Briefly described|p6|||of Cattle Creek Formation||||||
26754|Mount Aberdeen Volcanics|31984|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26754|Mount Aberdeen Volcanics|32553|4|Described|p44|||||||||
26754|Mount Aberdeen Volcanics|32556|4|Described|Table 3|||L.Perm.||||||
26754|Mount Aberdeen Volcanics|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
26754|Mount Aberdeen Volcanics|37613|5|Briefly described|p249|||See also Fig.3||||||
26754|Mount Aberdeen Volcanics|45151|6|Mentioned|Table 7|||||||||
26754|Mount Aberdeen Volcanics|48922|4|Described|p43|||L.Perm.||||||
26754|Mount Aberdeen Volcanics|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Andesite, dacite (with well-developed flow banding in places), rhyolite, dacitic ignimbrite, lithic-crystal tuff, crystal tuff, volcanic breccia.|
32041|Mount Alma Formation|22482|6|Mentioned|Fig.1|||||||||
32041|Mount Alma Formation|23468|5|Briefly described|p 296|||spelt "Mt" in text||||||
32041|Mount Alma Formation|23522|5|Briefly described|p250 Fig 6|Late Devonian|Middle Devonian|Mount is Mt. in text.||||||
32041|Mount Alma Formation|24399|4|Described|p275, p272 Fig. 1|Late Devonian|Late Devonian|Mount is Mt. in text.  Correlated with Crana beds. Dominated by monotonous sequences of thinly bedded siltstone and fine- medium-grained sandstone.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geol. Prov: New England Fold Belt.||||||
32041|Mount Alma Formation|24420|5|Briefly described|p6|Early Carboniferous|Late Devonian|Previously mapped as Crana beds.||||||
32041|Mount Alma Formation|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|24491|4|Described|p18|Late Devonian|Late Devonian|Formerly included in the Mount Holly beds, seperate due to differing radiometric signatures. Includes Unit B of the Crana beds, most of the Barmundoo beds, the Melrose beds as well as some rocks from Mount Holly beds.||||||
32041|Mount Alma Formation|24615|5|Briefly described|CD|Early Carboniferous|Late Devonian|[DCa].  Thinly interbedded fine-grained sandstone and siltstone and thick beds of conglomerate with andesitic to dacitic clasts and siltstone rip-up-clasts.||||||
32041|Mount Alma Formation|50197|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|50208|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|50209|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
32041|Mount Alma Formation|50213|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Thinly interbedded fine-grained sandstone and siltstone and thick beds of conglomerate with andesitic to dacitic volcanic clasts and siltstone rip-up clasts.||||||
32041|Mount Alma Formation|50317|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Thinly interbedded fine-grained sandstone and siltstone and thick beds of conglomerate with andesitic to dacitic volcanic clasts and sandstone rip-up clasts.||||||09-JUN-04
32041|Mount Alma Formation|60557|4|Described|p18 Fig. 5a, p22|Early Carboniferous|Late Devonian|Rhythmically interbedded sandstone and siltstone with conglomerates characterised by rip-up clasts.  Unconformably overlies the Craigilee beds; conformably overlain by Rockhampton Group.  See also p19-20 Figs. 5b,c.||||||09-JUN-05
32041|Mount Alma Formation|60705|5|Briefly described|p645, p655|Late Devonian|Late Devonian|Correlative of the Campwyn Volcanics in northern New England Fold Belt. Age: 361.2+/-6 Ma. Geological Province: Yarrol terrane. Mount is Mt in text.||||||12-APR-05
32041|Mount Alma Formation|61147|6|Mentioned|p376.|Early Carboniferous|Late Devonian?|Limestone olistoliths imply substantial, possibly continuous, carbonate sedimentation during much of the Devonian.||||||
32041|Mount Alma Formation|61392|5|Briefly described|p165 Fig. 2|Famennian|Frasnian|Part of the 'Bindawallah Stratigraphic Assemblage'.||||||07-FEB-11
32041|Mount Alma Formation|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Late Devonian|Includes the former Barmundoo Formation. Geological Province: Yarrol Province. Mount is Mt in text. See also p1000 Fig.3, p1006, p1028.||||||
32041|Mount Alma Formation|61778|5|Briefly described|p234 Fig. 1, p241|Early Carboniferous|Early Carboniferous|Mount is Mt in text. Geological Province: Berserker Subprovince.||||||07-FEB-11
32041|Mount Alma Formation|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Thinly interbedded fine-grained sandstone and siltstone and thick beds of conglomerate with andesitic to dacitic clasts and siltstone rip-up clasts.||||||
32041|Mount Alma Formation|64429|6|Mentioned|p16 Fig.1|Early Carboniferous|Late Devonian|Unconformably overlain by Berserker Group. Mount is Mt in text of figure.||||||
32041|Mount Alma Formation|65214|6|Mentioned|p282|Devonian|Devonian|QLD, Rockhampton. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
32041|Mount Alma Formation|65388|5|Briefly described|p69, 72, 439|late Devonian|Late Devonian|361+/- 5.2 Ma U-Pb LA-ICP-MS age (Bryan et al 2004). Part  of a belt of Silurian to early Carboniferous rocks.||||||
32041|Mount Alma Formation|68008|2|Defined|p79-90,p2,p11, p18, p20, p22-23, p25-26,|Tournaisian|Frasnian| Named and briefly described by the Yarrol Project Team (1997). Widespread unit. Includes the former Unit B of the Crana beds; the Melrose beds W of Ridgelands; much of the Mount Holly beds; most of the Barmundoo beds; and various undivided Silurian to Carboniferous rocks.  Named after Mount Alma. 640m thick at the type section, which is from GR279450 7349596 to GR278510 7349394 on the Bajool 100k sheet. Total thickness estimated between 3 and 5 km. Measured type section diagram. Details of a second, representative section are given. Subdued to very hilly topography. Intra-oceanic back-arc basin deposits. Lithology is described and illustrated in detail. Folds and cleavage vary in intensity locally.  Structural data discussed. Princhester Serpentinite is thrust over this unit. Micropaleontology table. Shelly fossils, coral species listed. Geophysics modelling. Is overlain by (and faulted against) Calliope beds, conformably to disconformably by Rockhampton Group, and unconformably by Casuarina beds, Lakes Creek Formation, Dalma and Alton Downs Basalts, Winterbourne and Mount Salmon Volcanics. Is intruded by Cecilwood and Bajool Quartz Diorites, Bundaleer and Zig Zag Tonalites, Kabra Quartz Monzodiorite, Bocoolima, Ridgelands, Diglum and Rocky Point Granodiorites, and Pack Granite. See also  p38-40, p61, p67, p71-73, p92, p106-107, p109, p113, p159, p162, p209, p246, p254, p261, p270, p275, p279, p307, p340, p353, p361, p366, p375, p381, p393, p395-396, p419, p423-424, p429, p477-479, p488, p490, p569, p573-575, p577, p581-582, p593, p603, p623, p628, p633, p648, p654-656.||||Unconformably overlies Calliope, Erebus, Craigilee beds and Raspberry Creek Formation. At least partly equivalent to Mount Hoopbound and Lochenbar Formations and Three Moon Conglomerate. See Comments.|Dominantly interbedded siltstone and fine-grained sandstone, with minor medium- to very coarse-grained sandstone and conglomerate, thin autochthonous limestone, and allochthonous limestone blocks (sourced from Erebus and Calliope beds).|05-SEP-18
32041|Mount Alma Formation|68359|6|Mentioned|p9|||||||||
32041|Mount Alma Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Balaclava, Lochenbar and Mount Hoopbound Formations, the Tanderra Volcanics,  the Channer Creek beds and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
32041|Mount Alma Formation|68679|3|Fully described|p312-314, p318, p337-341, p346-348, p350|Early Carboniferous|Late Devonian|See also p425-426, p468. Yarrol Project Team (1997). Northern New England Orogen. Previously part of the (now abandoned) Mount Holly beds (Murray et al., 2012). Comprises several previously mapped units, named or undifferentiated (listed on p340). A widespread unit: forms an arcuate, discontinuous belt 260km long and up to 30km wide, from the Fitzroy River NW of Ridgelands to Monto. The type section is at Mount Alma and along Takilberan Creek. Intraoceanic backarc basin deposits. No marine fossils: rare plant and trace fossils. Basal limestone blocks derived from underlying Erebus beds. RELATED UNITS (continued): Is intruded by Pack Granite, Zig Zag and Bundaleer Tonalites, Gavial Gabbro, Princhester Serpentinite, Bocoolima and Rocky Point Granodiorites, Kabra Quartz Monzodiorite, and Cecilwood Quartz Diorite and Bajool Quartz Diorite. ||||Is overlain unconformably by Berserker Group. Faulted against Capella Creek Group. Is thrust under the Erebus beds. May correlate with Tanderra Volcanics. See COMMENTS  for more.|Mainly thinly and rhythmically interbedded siltstone and fine-grained, fining-upwards sandstone, with local medium-grained to very coarse-grained sandstone and conglomerate with siltstone rip-up clasts. Minor micritic limestone.|
32041|Mount Alma Formation|69600|5|Briefly described|p655|Early Devonian|Early Devonian|Barker et al. (1997). Mount Etna region. Caves eroded in this unit contain fossil-bearing deposits including Pleistocene megafauna.||||||
32041|Mount Alma Formation|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
29538|Mount Alto Granite|23423|5|Briefly described|p311 Table 7.4||Early Permian|Mount Alto Supersuite. Hodgkinson Province.||||||
29538|Mount Alto Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 388. S-Type.||||||
29538|Mount Alto Granite|42968|6|Mentioned|p99|||Actually spelt Mt Alto Granite.||||||
29538|Mount Alto Granite|43259|4|Described|Appendix 1,p43.||Permian|||||||
29538|Mount Alto Granite|43625|4|Described|p54,127,Appendix 7|||||||||
29538|Mount Alto Granite|50387|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Kennedy Province. Age: 269 +/- 8 Ma, 271 +/- 5 Ma (SHRIMP). Of Mount Alto Supersuite||||||11-JUN-04
29538|Mount Alto Granite|60425|4|Described|p56 Tb. 4|Early Permian|Early Permian|Of Mount Alto Suite (Mount Alto Supersuite). Intrudes Hodgkinson Fm. Age: 269+/-8Ma, 271+/-5Ma (SHRIMP).S-type, med.-gr., slightly to moderately porphyritic (biotite-) garnet-tourmaline-muscovite granite; minor fluorite, apatite -  incl: lith.detail||||||07-FEB-11
29538|Mount Alto Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~9 km2 as several stocks and pods in the central Hodgkinson Province.|269 +/- 8 Ma and 271 +/- 5 Ma (SHRIMP).|Mount Alto Suite.|||Slightly to moderately porphyritic, (biotite-) garnet-tourmaline-muscovite and (garnet-) tourmaline-muscovite-biotite granite.|
36712|Mount Alto Suite|23423|5|Briefly described|p311 Table 7.4||Early Permian|Of Mount Alto Supersuite.||||||
36712|Mount Alto Suite|60425|5|Briefly described|p274-5 Appdx. 1|||Of Mount Alto Supersuite. Contains Mount Alto Granite. S-type.||||||07-FEB-11
36712|Mount Alto Suite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Brodies Camp, Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36712|Mount Alto Suite|69593|5|Briefly described|p478-480, p482, p505, p506 Fig.6.26|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~9 km2 as several stocks and pods in the central Hodgkinson Province. Geochronology by Davis, Henderson and Wysoczanski (1998).|269 +/- 8 Ma and 271 +/- 5 Ma (SHRIMP).||Mount Alto Granite.||Slightly to moderately porphyritic, (biotite-) garnet-tourmaline-muscovite and (garnet-) tourmaline-muscovite-biotite granite. Very strongly fractionated S-type.|
28783|Mount Alto Supersuite|22497|6|Mentioned|p113|||Mount is written MT in text||||||
28783|Mount Alto Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
28783|Mount Alto Supersuite|23423|4|Described|p311 Table 7.4||Early Permian|S-type granites. Intrudes Hodgkinson Formation. Also see p246-247. Hodgkinson Province.||||||
28783|Mount Alto Supersuite|23430|6|Mentioned|p493|||||||||
28783|Mount Alto Supersuite|42658|4|Described|p34|||||||||
28783|Mount Alto Supersuite|43285|5|Briefly described|Map Legend||Early Permian|||||||
28783|Mount Alto Supersuite|43625|4|Described|p54|||||||||
28783|Mount Alto Supersuite|50387|5|Briefly described|Map legend|Permian|Permian|Geological Province: Kennedy Province.||||||
28783|Mount Alto Supersuite|60425|4|Described|p56 Tb. 4, p83, p274-5 Appdx. |Early Permian|Early Permian|Contains Mount Alto Suite and its Mount Alto Granite. Intrudes Hodgkinson Formation. Age: 269+/-8Ma and 271+/-5Ma (SHRIMP). S-type, medium-grained, slightly to moderately porphyritic (biotite-)-granet-torumaline-muscovite granite.||||||07-FEB-11
28783|Mount Alto Supersuite|61527|5|Briefly described|p789|||Belt of granite plutons. Divided into the Mount Alto granite and Northedge granites. Geological Province: Hodgkinson Province. Mount is Mt in text||||||
28783|Mount Alto Supersuite|66852|5|Briefly described|pp938-939, p941.|||Written as Mt Alto in the text. The geometry of its plutons has been influenced by sinistral movement in the  WNW-ESE Desailly Structure, described in the article. Its plutons also display intimate spatial relationships with the Alto Fault Zone.||||||
28783|Mount Alto Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|||||S-type granitoids.|
24390|Mount Angelay Granite|22465|6|Mentioned|p934|||Author uses Mt Angelay igneous complex as an alternative term.||||||01-FEB-07
24390|Mount Angelay Granite|22515|3|Fully described|Fig1p398,402,404||Paleoproterozoic|||||||07-NOV-08
24390|Mount Angelay Granite|22667|6|Mentioned|Fig1 P234|||||||||
24390|Mount Angelay Granite|23545|5|Briefly described|p606 Table 1.|||||||||
24390|Mount Angelay Granite|23967|5|Briefly described|p1334|||Referred to as Mount Angelay Igneous Complex in text.||||||
24390|Mount Angelay Granite|24032|6|Mentioned|p6 Tb. 1, p16|||Mount is spelt Mt in table and text. Biotite and hornblende-biotite granite, porphyritic and non-porphyritic.||||||
24390|Mount Angelay Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24390|Mount Angelay Granite|24254|6|Mentioned|p17 Fig.1|||Mount is Mt in text. Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
24390|Mount Angelay Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Mount is Mt. in text. Geological Province: Mount Isa Block. Age: ~1528-1520Ma (U-Pb)||||||
24390|Mount Angelay Granite|24257|6|Mentioned|p65 Fig.1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
24390|Mount Angelay Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
24390|Mount Angelay Granite|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block. Mount is Mt in text.||||||
24390|Mount Angelay Granite|37862|4|Described|p589|||||||||
24390|Mount Angelay Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24390|Mount Angelay Granite|38658|6|Mentioned|p152|||||||||
24390|Mount Angelay Granite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24390|Mount Angelay Granite|39445|6|Mentioned|Table 2|||||||||
24390|Mount Angelay Granite|39496|4|Described|p15|||||||||
24390|Mount Angelay Granite|40840|6|Mentioned|Map legend|||||||||
24390|Mount Angelay Granite|43490|6|Mentioned|8|||||||||
24390|Mount Angelay Granite|44195|6|Mentioned|p357|||||||||
24390|Mount Angelay Granite|45161|5|Briefly described|p52|||||||||
24390|Mount Angelay Granite|45166|5|Briefly described|p39|||||||||
24390|Mount Angelay Granite|49009|2|Defined|p25|Proterozoic|Proterozoic|Mapped as Williams Granite by Carter and Opik, (1963).||||||15-MAR-07
24390|Mount Angelay Granite|50100|5|Briefly described|p21|Calymmian|Calymmian|Of the Williams Supersuite.||||||
24390|Mount Angelay Granite|50536|5|Briefly described|p1.5, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite.||||||
24390|Mount Angelay Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||27-AUG-04
24390|Mount Angelay Granite|61933|5|Briefly described|p169 Fig.1, p175|Mesoproterozoic|Mesoproterozoic|Age: 1530-1520 Ma.||||||
24390|Mount Angelay Granite|61936|5|Briefly described|p200|||A-type, metaluminous, magnetite-bearing plutonic rocks of the Isan Orogeny. Mount is Mt in text.||||||
24390|Mount Angelay Granite|63055|5|Briefly described|p11, p12 Fig. 1|||Mount is Mt in text.||||||01-FEB-07
24390|Mount Angelay Granite|64248|6|Mentioned|p45|||||||||
24390|Mount Angelay Granite|64249|6|Mentioned|p102|Mesoproterozoic|Mesoproterozoic|Age: 1520 and 1536Ma. Further south than Saxby Granite.||||||22-APR-09
24390|Mount Angelay Granite|64250|6|Mentioned|p9 fig 1, p11 fig 3|||Cloncurry Fold Belt, Mount Isa Inlier.|1529 +/-4 Ma; 1523 +/-4 Ma.|||||
24390|Mount Angelay Granite|64251|6|Mentioned|p62 Fig. 9|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
24390|Mount Angelay Granite|65396|5|Briefly described|p7, p22, p40, p53, p56, p61, p82, p84|Calymmian|Calymmian|See also p88, p157, p172, p175, p179, p224, p241, p280, p283-284, p327, p359-361, p364-368, p388, p393, p438, p440, p444-445, p455-491. Cloncurry Fold Belt: Eastern succession; Williams-Naraku Batholith. Magnetic and gravity worms discussed. Fluid inclusions studied. Stress partitioning and fluid flow models detailed.|1529 +/- 4 Ma, 1523 +/- 4 Ma (SHRIMP)||||Hornblende(-quartz) monzogranite.|
24390|Mount Angelay Granite|65755|5|Briefly described|p3|||Written Mt in text. 1530 - 1520 Ma||||||
24390|Mount Angelay Granite|66913|5|Briefly described|p171 fig 2, p188|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2.||||||
24390|Mount Angelay Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p20|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot. Williams Igneous Event. Forms a large (25 x 5 km) pluton in the south of the Doherty-Fig Tree Gully Domain. Strong magneic response. Age determinations of a monzogranite constituent by Pollard and McNaughton (1997).|1529 +/- 4 Ma and 1524 +/- 4 Ma.|Williams Supersuite.|||Equigranular to porphyritic biotite, hornblende and hornblende-biotite granite, locally foliated; minor pyroxene-bearing granite, granodiorite, leucogranite, aplite. I-type.|
24390|Mount Angelay Granite|67498|5|Briefly described|p918 Fig. 1, p919, p926|||||Of the Williams Granite Suite||Intrudes the Corella Formation.||
24390|Mount Angelay Granite|69056|6|Mentioned|Time-Space plot sheet|Calymmian|Calymmian||1524 +/- 14 Ma.|||||
24390|Mount Angelay Granite|69591|5|Briefly described|p51, p59|||Eastern Mount Isa Province; late Isan Orogeny.|1529 +/- 4 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.|||Equigranular to porphyritic biotite, hornblende and hornblende-biotite granite, locally foliated; minor pyroxene-bearing granite, granodiorite, leucogranite, aplite. A-type.|
24390|Mount Angelay Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny. The two facies associations are mapped separately.||Williams Supersuite.|||Equigranular to porphyritic biotite, hornblende and hornblende-biotite granite, locally foliated; minor pyroxene-bearing granite, granodiorite, leucogranite, aplite. Hornblende diorite to tonalite; commonly associated with net-veining.|05-MAY-16
24390|Mount Angelay Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes an unnamed hornblende diorite-tonalite; commonly associated with net veining.||Williams Supersuite.|||Equigranular to porphyritic biotite, hornblende and hornblende-biotite granite, locally foliated; minor pyroxene bearing granite, granodiorite, leucogranite, aplite.|
24390|Mount Angelay Granite|71592|5|Briefly described|Appendix A.|||Doherty-Fig Tree Gully Domain, Mount Isa Orogen.|1529+/-4 Ma (crystallisation: zircon U-Pb SHRIMP)||||Granite.|
32147|Mount Appenben Granite|23037|5|Briefly described|p72,3|Permian|Carboniferous|Intrudes the Boam Creek Granodiorite.||||||
32147|Mount Appenben Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgma].  Pink to grey, medium- to fine-grained biotite granite.||||||
32147|Mount Appenben Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to grey, medium- to fine-grained, biotite granite.||||||18-MAY-04
32147|Mount Appenben Granite|65388|3|Fully described|p267-268, p236 Fig. 81, p244, 245, 255|Early Permian|Late Carboniferous|Auburn Arch. Appears to intrude Boam Creek Quartz Monzodiorite. Geophysical response and lithology compared with Broadlands Granite, fractionation with Glenleigh Granite.  Age uncertain. Pink to grey, fine to medium-grained biotite granite.||||||
32147|Mount Appenben Granite|68679|5|Briefly described|p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Boam Creek Quartz Monzodiorite.|Pink to grey, fine- to medium-grained biotite granite.|
70398|Mount Bania Granite|64556|6|Mentioned|p56|||Age: 228.5+/-2.1Ma. On ROSEDALE sheet.||||||07-FEB-11
70398|Mount Bania Granite|65452|5|Briefly described|p7 Tb.2|Late Triassic|Middle Triassic|SHRIMP U-Pb zircon magmatic crystallisation age.|228.5 +/- 2.1 Ma (Black; unpublished).||||Fine- to medium-grained, granophyric, porphyritic, biotite hornblende monzogranite.|
70398|Mount Bania Granite|67203|5|Briefly described|p2-4|Late Triassic|Late Triassic|One of several intrusives emplaced around the time of Agnes Water Volcanics.|228.5 +/- 2.1 Ma (Black, unpublished).||||Fine-to medium-grained, granophyric, porphyritic, biotite-hornblende monzogranite.|
70398|Mount Bania Granite|68421|5|Briefly described|Map Legend|Carnian|Norian|Triassic Igneous Province. Zircon U-Pb age.|228.5 +/- 2.1 Ma (Black et al. 2005)||||Pink, medium-grained, porphyritic hornblende-biotite monzogranite with scattered inclusions of fine-grained, pale grey granite to 3 cm; medium-grained, equigranular hornblende quartz syenite; pale grey medium-grained hornblende granodiorite.|
70398|Mount Bania Granite|68679|5|Briefly described|p428, p431-432|Late Triassic|Late Triassic|Northern New England Orogen; Monto area.|228.5 +/- 2.1 Ma (SHRIMP U-Pb: Black, unpub).||||Pink, medium-grained, porphyritic hornblende-biotite monzogranite with scattered fine-grained granite inclusions; medium-grained, equigranular hornblende quartz syenite; pale grey, medium-grained hornblende granodiorite.|
41938|Mount Bassett Dolerite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|basalt and dolerite dyke swarm (with screens of Carmila beds, Whitsunday Volcanics, Campwyn beds and/or Calen Coal Measures).||||||
41938|Mount Bassett Dolerite|65388|2|Defined|p410-412, p403 Fig. 135, p419, 420|Cretaceous|Cretaceous|Appears to intrude Whitsunday Volcanics, Carmila beds and Campwyn Volcanics. Likely age given. Dominantly very dark grey to black, aphyric to porphyritic dolerite with dykes of quartz diorite or quartz monzodiorite in type locality (quarry).||||||
36521|Mount Benjonney complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 171.||||||
32161|Mount Benmore Volcanics|23037|4|Described|p17,19-24,27-30,9,49|Permian|Late Carboniferous|Possible correlation with Camboon Volcanics, and Lizzie Creek Volcanics. Of "Connors Volcanics". Underlying unit Leura Volcanics (non-con).||||||
32161|Mount Benmore Volcanics|23042|4|Described|p25,7,8,32-5,54,Fig2||Early Permian|Overlying unit Carmila beds. Underlying unit Leura Volcanics.||||||
32161|Mount Benmore Volcanics|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pvb].  Basalt ot basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite;  minor felsic lava and volcaniclastics.||||||
32161|Mount Benmore Volcanics|50213|5|Briefly described|Map legend|Permian|Permian|Basalt to basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.  Overlie the Leura Volcanics.||||||17-MAY-04
32161|Mount Benmore Volcanics|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Basalt to basaltic andesite, volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics. Overlies: Leura Volcanics. Underlies: Back Creek Group.||||||28-MAY-08
32161|Mount Benmore Volcanics|60472|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Basalt to basaltic andesite, volcaniclastic sandstone and rudite; minor felsic lava and felsic volcaniclastic rocks.||||||
32161|Mount Benmore Volcanics|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Basalt to basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.||||||17-SEP-04
32161|Mount Benmore Volcanics|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Basalt to basaltic andesite, volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.||||||
32161|Mount Benmore Volcanics|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Includes: Cerberus Rhyolite Member. Basalt to basaltic andesite, volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.||||||
32161|Mount Benmore Volcanics|60557|5|Briefly described|p20 Fig. 5c, p24|Early Permian|Late Carboniferous|Bimodal in composition, comprising basalt to basaltic andesite with locally dominant rhyolite and dacite, and subordinate volcaniclastics.||||||09-JUN-05
32161|Mount Benmore Volcanics|60787|5|Briefly described|p9|Permian|Permian|||||||
32161|Mount Benmore Volcanics|61035|4|Described|p7|Early Permian|Late Carboniferous|Of Lizzie Creek Volcanic Group. Underlain by Leura Volcanics. Age: ~291Ma (Withnall et al., 1998a,b; Hutton et al., 1999). Consists of basalt to basaltic andesite lava, volcaniclasic sandstone + rudite. Geol Prov: Connors Sudprovince.||||||07-FEB-11
32161|Mount Benmore Volcanics|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Basalt and basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.||||||
32161|Mount Benmore Volcanics|65388|3|Fully described|p117-126; p119, 20, 31, 84, 85, 86, 91|Artinskian|Early Permian|Major component of Lizzie Creek Volcanic Group, Connors Arch. Includes Cerberus Rhyolite Member. Originally included in Connors Volcanics. Overlie the Leura Volcanics, Tartrus Rhyolite (conformable), Coppermine Andesite, Macksford Andesite, Cerberus Rhyolite Member; overlain by Carmila beds or Back Creek Group. Hornsfelsed by Waitara Granite. SHRIMP date on interbedded Ignimbrite: 284.7+/- 4.4 Ma.  Lithologically identical to Macksford Volcanics. May be equivalent in part. Basalt flows and volcanic sandstone and poorly sorted volcanic rudite. Intruded by unnamed gabbro. See also p104, 106, 108, 110, 111, 112, 114, 128, 135-141, 143, 175, 176, 187, 338, 362, 380, 391, 399, 437, 441.||||||
32161|Mount Benmore Volcanics|68679|3|Fully described|p338, p353, p355, p357-360|Artinskian|Sakmarian|Withnall et al. (1998, 2009). Connors Subprovince, New England Orogen. Previously mapped, at least partly, as Connors Volcanics; but is dominated by basaltic lavas and clastic rocks compared with the rhyolitic ignimbrites of the Connors Volcanics. Is continuous with rocks originally mapped as Lizzie Creek Volcanics. A source of sediments in Goodedulla beds. RELATED UNITS (continued): Is overlain by the Tiverton Formation, Langdale Hill Rhyolite (transgressively/?unconformably), Carmila and Goodedulla beds or Back Creek Group.|284.7 +/- 4.4 Ma (Fanning et al., 2009).|Lizzie Creek Volcanic Group.|Cerberus Rhyolite Member.|Overlies, is folded with and thrust against Leura Volcanics. Overlies Tartrus, Cobweb Mountain Rhyolites, Coppermine and Macksford Andesites. May correlate with Ametdale Volcanics. See COMMENTS.|Mostly basaltic andesite or basalt lavas, commonly autobrecciated and altered to epidote and chlorite; subordinate, generally coarse volcaniclastic rocks: poorly sorted polymict conglomerates and sandstones. Rare felsic thin ignimbrite sheets.|
32161|Mount Benmore Volcanics|73036|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Basalt to basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.|
32161|Mount Benmore Volcanics|73037|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Basalt to basaltic andesite (commonly autoclastic), volcaniclastic sandstone and rudite; minor felsic lava and volcaniclastics.|
23813|Mount Boddington Granite|22847|3|Fully described|p 42|||Spelt "Mt" in text instead of Mount||||||
23813|Mount Boddington Granite|23422|5|Briefly described|p172, p209 Table 6.6|Middle Ordovician|Middle Ordovician|Of Lavery Creek Supersuite.||||||
23813|Mount Boddington Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 88. I-Type.||||||
23813|Mount Boddington Granite|42750|2|Defined|p38||Middle Ordovician|||||||
23813|Mount Boddington Granite|43093|4|Described|Appendix 1||Ordovician|Middle Ordovician||||||
23813|Mount Boddington Granite|43259|4|Described|Appendix 1,p21.||Ordovician|Middle Ordovician.||||||
23813|Mount Boddington Granite|43933|5|Briefly described|Map Legend||Ordovician|||||||
23813|Mount Boddington Granite|62521|5|Briefly described|p9, p26|Middle Ordovician|Late Cambrian|Of the Lavery Creek Supersuite. Geological Province: Ravenswood Batholith. Medium-grained, pink to red, biotite granite.; quartz rich.||||||14-JAN-08
23813|Mount Boddington Granite|68731|6|Mentioned|p149|||Included in a composite Rb-Sr isochron that indicated an age of 470 +/- 30 Ma (Webb 1969b); this study questions this analysis in determining the age of individual plutons.||||||17-JUL-14
70141|Mount Bridgman Igneous Complex|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Greenish-grey med-coarse-gr. hornblende gabbro; dark grey, fine-gr.diorite, quartz microdiorite, porphyritic microdiorite; pink to light-grey, med.-coarse-gr. biotite monzogranite to syenite and leucogranite; minor aplite dykes.||||||
70141|Mount Bridgman Igneous Complex|65388|2|Defined|p412-413, p403 Fig. 135, p420|Early Cretaceous|Early Cretaceous|Intrudes and has hornfelsed Carmila beds. Age assumed same as lithologically similar Ben Mohr Igneous Complex. Dark pink, medium-grained porphyritic syenogranite at type locality.||||||
33143|Mount Buffalo Rhyolite|23042|4|Described|p26,31,39-41|Early Permian|Late Carboniferous|||||||
33143|Mount Buffalo Rhyolite|60475|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Felsic (mainly rhyolitic) volcaniclastic sandstone, conglomerate, breccia and siltstone(tuff); minor rhyolitic ignimbrite and flows.||||||
33143|Mount Buffalo Rhyolite|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Felsic (mainly rhyolitic) volcaniclastic sandstone, conglomerate, breccia and siltstone; rhyolitic ignimbrite; minor rhyolite flows.||||||
33143|Mount Buffalo Rhyolite|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Felsic volcaniclastic sandstone, conglomerate, breccia and siltstone; minor crystal rich to crystal poor and lithic rich to lithic poor rhyolitic ignimbrite; local rhyolite flows.||||||
33143|Mount Buffalo Rhyolite|65388|6|Mentioned|p127, 128|||Misspelling of Mount Buffalo Volcanics. Overlies Ametdale Volcanics. Possible correlative of Cobweb Mountain Rhyolite.||||||
33143|Mount Buffalo Rhyolite|68679|5|Briefly described|p353|||Connors-Auburn Province.||Lizzie Creek Volcanic Group.||||
35013|Mount Bulgi Conglomerate Member|23037|4|Described|p30,1, 4-6, 40, 80|Early Permian|Late Carboniferous|Underlying unit Camboon Volcanics.||||||
35013|Mount Bulgi Conglomerate Member|24615|5|Briefly described|CD|Early Permian|Early Permian|[CPvcb].  Polymictic conglomerate and subordinate sandstone containing mainly felsic volcanic clasts and locally granite clasts.||||||
35013|Mount Bulgi Conglomerate Member|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|?Of the Camboon Volcanics?||||||17-MAY-04
35013|Mount Bulgi Conglomerate Member|50215|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Camboon Volcanics.Polymictic conglomerate and subordinate sandstone containing mainly felsic volcanic clasts and locally granite clasts.||||||18-JUN-09
35013|Mount Bulgi Conglomerate Member|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Camboon Volcanics.  Polymictic conglomerate and subordinate sandstone containing mainly felsic volcanic clasts and local granite clasts.||||||
35013|Mount Bulgi Conglomerate Member|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Camboon Volcanics.||||||
35013|Mount Bulgi Conglomerate Member|60282|5|Briefly described|p6, p19|||Basal unit of Camboon Volcanics, mapped separately in the Torsdale area.  Contains mainly felsic volcanics and granite clasts.||||||28-APR-05
35013|Mount Bulgi Conglomerate Member|61777|5|Briefly described|p228, p230|||Withnall et al., 1998. Of Camboon Volcanics basal unit. Overlies Torsdale Volcanics. Consists of felsic volcanic and some granite clasts.||||||07-FEB-11
35013|Mount Bulgi Conglomerate Member|65388|4|Described|p21-23, p14, 15, 19, 20, 28, 31, 50, 264|||Auburn Arch. Base of Camboon Volcanics. Unconformably overlies Torsdale Volcanics and Glenhalvern Granite in the Banana Range. Disconformably overlies Kooingal Granodiorite Complex. Derived from Torsdale Volcanics but includes clasts of the granite that intrudes Torsdale Volcanics too. Correlated with Youlambie Conglomerate of Yarrol Province.||||||
35013|Mount Bulgi Conglomerate Member|68679|5|Briefly described|p352, p354, p407|||SW of Biloela; Auburn Arch, northern New England Orogen. Its position directly ovelying granitoids indicates a hiatus between the Torsdale and Camboon Volcanics. Appears as Bulgi Conglomerate Member on p407.||Basal Camboon Volcanics.||Nonconformably overlies Torsdale Volcanics and Glenhalvern Granite; disconformably overlies Kooingal Granodiorite Complex.|Polymictic pebble to boulder conglomerate lenses. Clasts derived from the Torsdale Volcanics and the granitoids that intrude them.|
69203|Mount Bullaganang Granite|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Pale pink to pale brownish pink, medium-grained, uneven-grained, leucocratic biotite syenogranite; moderate to high magnetic response.||||||11-DEC-07
69203|Mount Bullaganang Granite|63748|6|Mentioned|p68, p69|||Probably misspelt - should be Bullaganang Granite.||||||07-FEB-11
69203|Mount Bullaganang Granite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Jibbinbar, Mount You You and Palgrave Granites; Boxwell and Greymare Granodiorites; are all mapped under the symbol, Pgn.||||||
69203|Mount Bullaganang Granite|71628|6|Mentioned|p5: 4|||Purdy et al. (2007). Now Mount Bullaganang Leucosyenogranite.||||||
22399|Mount Canton Igneous Complex|22847|3|Fully described|p 57|Permian|Carboniferous|||||||
22399|Mount Canton Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
22399|Mount Canton Igneous Complex|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22399|Mount Canton Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 494. I-Type.||||||
22399|Mount Canton Igneous Complex|43093|4|Described|Appendix 1|Permian|Carboniferous|||||||
22399|Mount Canton Igneous Complex|43259|4|Described|Appendix 1,p7&p51|Permian|Carboniferous|||||||
22399|Mount Canton Igneous Complex|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22399|Mount Canton Igneous Complex|69593|5|Briefly described|p491, p494-495|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. An intrusive-extrusive Complex, commonly associated with intrusives of the Leichhardt Supersuite.||Leichhardt Suite.|||Rhyolitic and dacitic ignimbrite; rare andesitic ignimbrite and lava, and andesitic to rhyolitic volcaniclastics. I-type.|
36453|Mount Carbine Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|280-265 Ma.|Unit in Whypalla Supersuite.||||
36453|Mount Carbine Granite|23423|5|Briefly described|p247|||See also p284, p286. Whypalla Supersuite||||||
36453|Mount Carbine Granite|23430|5|Briefly described|495p|||||||||
36453|Mount Carbine Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 386.  S-Type.||||||
36453|Mount Carbine Granite|24086|6|Mentioned|p312 Fig. 1|||Mount is Mt. in text.||||||
36453|Mount Carbine Granite|50387|5|Briefly described|Map Legend|Permian|Permian| Of the Whypalla Supersuite.  Age: 280+/-7Ma (Rb-Sr).  Geological Province: Kennedy Province.||||||23-JUN-04
36453|Mount Carbine Granite|60425|4|Described|p80, p185, p187, p276-7 Appdx. 1|Early Permian|Early Permian|Of Mount Carbine Suite (Whypalla Supersuite). S-type. Age: 280+/-7Ma (Rb-Sr). Mod'ly to highly porphyritic (garnet-tourmaline-) muscovite-biotite granite - extensively deformed in places. Detailed lithology included (p277)||||||07-FEB-11
36453|Mount Carbine Granite|66852|6|Mentioned|p938 Fig.2, p939.|||Written as Mt Carbine in text. Cut by major WNW-ESE trending lineaments but with very little offset.||||||
36453|Mount Carbine Granite|69593|5|Briefly described|p479, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 Ma.|Mount Carbine Suite.|||S-type.|
69321|Mount Carbine Suite|60425|5|Briefly described|p274-7 Appdx. 1|Early Permian|Early Permian|Of Whypalla Supersuite. Contains Spurgeon and Mount Carbine Granites and an unnamed unit of biotite microgranite. S-type.||||||07-FEB-11
69321|Mount Carbine Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Mount Carbine, Spurgeon Granites.|||
29319|Mount Cardwell Granite|23291|5|Briefly described|p101 Tb. 3.13|Early Permian|Late Carboniferous|Parent: California Creek Suite. Age: 295-302Ma (Black, 1980). Intrudes Martin Creek Microgranite; intruded by Sandy Tate & Opah Granites, Campbell Creek granodiorite. Geological Province: Georgetown Region.||||||08-JUL-15
29319|Mount Cardwell Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
29319|Mount Cardwell Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 375. I-Type.||||||
29319|Mount Cardwell Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29319|Mount Cardwell Granite|23624|4|Described|p12|Permian|Carboniferous|Parent: Ootann Supersuite.||||||01-JUL-15
29319|Mount Cardwell Granite|43087|6|Mentioned|p37|||Reserved as Mount Cardwell Adamellite.||||||
29319|Mount Cardwell Granite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
29319|Mount Cardwell Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of California Creek Suite (Ootann Supersuite). I-type. Pink to cream med.-gr.,slightly porphyritic biotite granite, extensively altered in places; minor fine-gr. granite; probably consists of more than one major intrusion; extends into Georgetown region.||||||01-JUL-15
29319|Mount Cardwell Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium-grained, slightly porphyritic biotite monzogranite; minor fine-grained monzogranite?|
29319|Mount Cardwell Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium-grained, slightly porphyritic biotite monzogranite; minor fine-grained monzogranite?|
75655|Mount Cauley Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, fine to medium-grained, uneven-grained to slightly porphyritic, very leucocratic muscovite-biotite syenogranite; extensively deformed and partly recrystallised.|
75671|Mount Cavana beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Connors Subprovince. This unit, as well as the Inkerman Metamorphics and Key Creek Gneiss, are all mapped under the symbol, DCi.||||||
75671|Mount Cavana beds|68679|6|Mentioned|p347, p364|Carboniferous|Late Devonian|Northern New England Orogen.||||||
75671|Mount Cavana beds|68901|6|Mentioned|p2 Fig. i|Carboniferous|Late Devonian|New England Orogen.
||||||27-SEP-18
75671|Mount Cavana beds|69952|6|Mentioned|p85|Carboniferous|Late Devonian|New England Orogen.||||||
35185|Mount Chelona Granite|23042|5|Briefly described|p88,9, Fig 2|Cretaceous|Jurassic|Intrudes Campwyn Volcanics.||||||
35185|Mount Chelona Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35185|Mount Chelona Granite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Pale pink, medium- to coarse-grained, moderately porphyritic biotite monxogranite to granodiorite with minor mafic xenoliths; intruded by irregular pegmatite dykes.||||||16-MAR-06
35185|Mount Chelona Granite|65388|2|Defined|p414, 415, p403 Fig. 135|Cretaceous|Cretaceous|Intrudes poorly-exposed rocks of the Mountain View Volcanics. Interpreted age given. Pale pink, medium to coarse-grained, moderately porphyritic, biotite monzogranite or possibly granodiorite; moderately altered.||||||
78961|Mount Christian Granodiorite|65388|3|Fully described|p422|Neogene|Early Cretaceous|Sill-like body. Intruding Carmila beds. Age poorly constrained. Pale grey, fine-grained, slightly porphyritic, leucocratic biotite granodiorite.||||||
40127|Mount Clairvoyant Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Cgml].  Foliated, medium-grained porphyritic bitote granite.||||||
40127|Mount Clairvoyant Granite|50214|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
40127|Mount Clairvoyant Granite|61087|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Foliated, medium-grained porphyritic biotite granite.||||||
40127|Mount Clairvoyant Granite|65388|4|Described|p241-242, 272, 280, 340|Carboniferous|Carboniferous|New name. Auburn Province. Rocks previously included in Crystal Vale Adamellite. In contact with  younger Glencoe Gabbro, which may have caused some recrystallisation. Foliated medium-grained biotite granite grading into orthogneiss. Age is uncertain, but a Carboniferous age is likely.||||||
40127|Mount Clairvoyant Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Auburn Subprovince. This unit, as well as the Carinya Granite, Donore Granite Gneiss and Horse Granite Gneiss, are all mapped under the same symbol, Cga.||||||
40127|Mount Clairvoyant Granite|68679|5|Briefly described|p312, p406, p419|Carboniferous|Carboniferous|Northern New England Orogen. Could be related to Donore Granite Gneiss.||||May be intruded by Glencoe Gabbro.|Foliated, medium-grained porphyritic biotite granite; grades into orthogneiss with discontinuous biotite layers and lenticles.|
29342|Mount Clara beds|22845|2|Defined|p17,34,46-55,61,76,7||Early Carboniferous|Correlates with Amamoor beds||||||
29342|Mount Clara beds|22846|6|Mentioned|p14,18,20,68||Carboniferous|||||||
29342|Mount Clara beds|23251|6|Mentioned|p29|||In GOOMERI. A possible correlative of Amamoor beds.||||||
29342|Mount Clara beds|23799|6|Mentioned|p18|||Geological Province: D'Aguilar Province.||||||
29342|Mount Clara beds|43588|6|Mentioned|p30||Late Devonian|||||||
29342|Mount Clara beds|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
29342|Mount Clara beds|68679|6|Mentioned|p411|||||||Is intruded by One Mile Creek Granite.||
24393|Mount Cobalt Granite|22515|3|Fully described|Fig1p398,402-3,406||Paleoproterozoic|||||||07-NOV-08
24393|Mount Cobalt Granite|23967|6|Mentioned|p1331|||||||||
24393|Mount Cobalt Granite|23974|6|Mentioned|p1452 Fig. 2a|||Geological Province: Selwyn region.||||||
24393|Mount Cobalt Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24393|Mount Cobalt Granite|24256|6|Mentioned|p48, p50 Fig.2|||Mount is Mt. in text. Geological Province: Mount Isa Block.||||||
24393|Mount Cobalt Granite|37862|4|Described|p589|||||||||
24393|Mount Cobalt Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24393|Mount Cobalt Granite|38658|6|Mentioned|p152|||||||||
24393|Mount Cobalt Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24393|Mount Cobalt Granite|39043|6|Mentioned|p9|||||||||
24393|Mount Cobalt Granite|39445|6|Mentioned|Table 2|||||||||
24393|Mount Cobalt Granite|40840|6|Mentioned|Map legend|||||||||
24393|Mount Cobalt Granite|41306|6|Mentioned|p4|||||||||
24393|Mount Cobalt Granite|45161|5|Briefly described|p52|||||||||
24393|Mount Cobalt Granite|45166|5|Briefly described|p39|||||||||
24393|Mount Cobalt Granite|49009|2|Defined|p26|Proterozoic|Proterozoic|Mapped as Williams Granite by Carter & Opik (1963).||||||01-FEB-07
24393|Mount Cobalt Granite|50100|5|Briefly described|p21, p61|Calymmian|Calymmian|Of the Williams Supersuite.||||||
24393|Mount Cobalt Granite|50536|5|Briefly described|p1.5, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite.||||||
24393|Mount Cobalt Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
24393|Mount Cobalt Granite|65396|6|Mentioned|p61, p360|||Cloncurry District.|Between 1530 Ma and 1500 Ma.|||||
24393|Mount Cobalt Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event.||Williams Supersuite|||Equigranular biotite granite.|
24393|Mount Cobalt Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Equigranular biotite granite.|
24393|Mount Cobalt Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular biotite granite.|20-JAN-22
24393|Mount Cobalt Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular biotite granite.
|
24393|Mount Cobalt Granite|72889|6|Mentioned|p8, p39.|||||||||
40128|Mount Cooper Trachyte|24615|5|Briefly described|CD|Late Cretaceous|Late Cretaceous|[Kvc].  Alkali trachyte flows, tuff and breccia; some microsyneite dykes.||||||
40128|Mount Cooper Trachyte|50215|5|Briefly described|Map Legend|Late Cretaceous|Late Cretaceous|Alkali trachyte flows, tuff and breccia; some microsyenite dykes.||||||18-JUN-09
40128|Mount Cooper Trachyte|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit is mapped with Mount Salmon Volcanics under the symbol, Kvs.||||||
40128|Mount Cooper Trachyte|68679|6|Mentioned|p312-313, p347|Cretaceous|Cretaceous|Northern New England Orogen.||||||
40128|Mount Cooper Trachyte|73450|4|Described|p4, p55-56, p58|Campanian|Cenomanian|Comprises a series of prominent forested hills east of Baralaba; rocks are deeply weathered. Derived from a vent located at the western end of Mount Cooper. Lava dome (approaching granophyre in composition and texture) occupies the vent area. Maximum thickness is 120 m; strata dips outwards away from the dome. Ring dyke has a steep inward dip towards dome. Unpublished U-Pb zircon ages include 93.9 +/- 3 Ma and 93.4 +/- 5 Ma from more mafic rocks and 77.7 +/- 4 Ma from felsic rocks (Withnall et al., 2009).|ca 94-77 Ma||||Rhyolite and trachyte dykes, small pods of granite, pegmatite, and conglomerate with cobble- to boulder-sized sub-rounded to sub-angular clasts of trachyte, intermediate volcanics and fine-grained sedimentary rocks.|
75643|Mount Crompton Granodiorite|68679|5|Briefly described|p362, p365 Fig.5.49|Pennsylvanian|Pennsylvanian|Urannah Batholith, Northern Connors Subprovince. Deformed (well-developed foliation) and partly recrystallised.|308.1 +/- 1.9 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75643|Mount Crompton Granodiorite|69952|5|Briefly described|p2 Tb.i, p5, p89-|Carboniferous|Carboniferous|Urannah Batholith, SW of Bowen. SHRIMP U-Pb zircon magmatic crystallisation age.|307.9 +/- 2.6 Ma (Cross et al., 2015).|||Is intruded by Amelia Creek Tonalite.||30-NOV-15
75643|Mount Crompton Granodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|308+/-2.6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
75643|Mount Crompton Granodiorite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Grey or pale grey to pale pinkish grey, fine to medium-grained, uneven-grained to slightly porphyritic, (hornblende) biotite granodiorite to hornblende-biotite tonalite, and biotite monzogranite; commonly foliated.|
39553|Mount Cross Igneous Complex|23799|3|Fully described|p60, p61 Fig. 4|Permian|Carboniferous|Current mapping includes only the gabbros and derived grabroic sediments of the "Mount Cross Gabbro Complex" (Smith, 1974).  See also p14 Tb. 1.||||||03-DEC-21
39553|Mount Cross Igneous Complex|23800|5|Briefly described|Map legend|Permian|Carboniferous|||||||
39553|Mount Cross Igneous Complex|24560|5|Briefly described|Map legend|Permian|Carboniferous|Gabbroic intrusions, volcaniclastics (gabbro-derived sediments).||||||
39553|Mount Cross Igneous Complex|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|||||||
39553|Mount Cross Igneous Complex|68679|5|Briefly described|p351, p405|||North of Helidon, Yarraman Subprovince.||||Intrudes, and is faulted against, the Alice Creek beds.|Medium- to coarse-grained, extensively altered gabbro and sedimentary rocks derived directly from the gabbro.|
22406|Mount Cuthbert Granodiorite|22847|3|Fully described|p 53|Early Devonian|Late Silurian|||||||
22406|Mount Cuthbert Granodiorite|23422|5|Briefly described|p176, p214 Table 6.8|||Of Barrabas Supersuite.||||||
22406|Mount Cuthbert Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22406|Mount Cuthbert Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 208. I-Type.||||||
22406|Mount Cuthbert Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
22406|Mount Cuthbert Granodiorite|43259|4|Described|Appendix 1,p30.|Early Devonian|Late Silurian|||||||
22406|Mount Cuthbert Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22406|Mount Cuthbert Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Mount Cuthbert gdrt.||Unit in Barrabas Supersuite.||||
22406|Mount Cuthbert Granodiorite|64852|5|Briefly described|Map legend|Devonian|Silurian|Grey, fine- to medium-grained, hornblende-biotite granodiorite and tonalite.||||||
22406|Mount Cuthbert Granodiorite|69592|5|Briefly described|p293|||Southeast Ravenswood Batholith, Charters Towers Province.||Barrabas Supersuite.|||High-K and high-Rb granitoids.|
22406|Mount Cuthbert Granodiorite|70740|4|Described|p40|Early Devonian|Middle Silurian|Outcrop characteristics discussed. A type area is mentioned and described. Petrography in the type area is described. ||Barrabas Supersuite||Overlies the Kedumba Granodiorite.|Grey granodiorite and a grey, medium-grained, biotite-hornblende tonalite.|
26050|Mount Darcy Microgranodiorite|23291|5|Briefly described|p98 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Cumberland Range area. Geological Province: Georgetown Region.||||||08-JUL-15
26050|Mount Darcy Microgranodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 13. I-Type.||||||
26050|Mount Darcy Microgranodiorite|36216|2|Defined|p212|Carboniferous|Carboniferous|||||||
26050|Mount Darcy Microgranodiorite|38366|4|Described|p39|||||||||
26050|Mount Darcy Microgranodiorite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26050|Mount Darcy Microgranodiorite|40860|5|Briefly described|p116|||||||||
26050|Mount Darcy Microgranodiorite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
26050|Mount Darcy Microgranodiorite|43740|4|Described|p23|||||||||
26050|Mount Darcy Microgranodiorite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Hornblende-biotite granodiorite; biotite and hornblende-biotite microgranite.||||||05-JUL-04
26050|Mount Darcy Microgranodiorite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey, abundantly porphyritic biotite and hornblende-biotite microgranodiorite; locally brecciated, polymictic with clasts of basement granite and metamorphic rocks.|
26050|Mount Darcy Microgranodiorite|69593|5|Briefly described|p490, p511|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Cumberland Range Volcanic Group. Sm-Nd isotope data tabulated.|330 Ma.||||Hornblende-biotite and biotite microgranite to microtonalite. I-type.|
27049|Mount Departure Microgranite|23291|5|Briefly described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Newcastle Range A-types. Geological Province: Georgetown Region.||||||08-JUL-15
27049|Mount Departure Microgranite|23510|5|Briefly described|Map Legend||Early Permian|||||||
27049|Mount Departure Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 11. Assumed to be I-Type.||||||
27049|Mount Departure Microgranite|23619|4|Described|p39 Table 2||Carboniferous|Intrudes Cumbana Rhyolite. Overlying unit Undara Basalt. Georgetown Province.||||||
27049|Mount Departure Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27049|Mount Departure Microgranite|40542|6|Mentioned|p97|||||||||
27049|Mount Departure Microgranite|43113|4|Described|Table 2 p25||Carboniferous|||||||
27049|Mount Departure Microgranite|43253|5|Briefly described|map legend||Carboniferous|||||||
27049|Mount Departure Microgranite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
27049|Mount Departure Microgranite|43740|4|Described|p16|||||||||
27049|Mount Departure Microgranite|44926|5|Briefly described|Map Legend|||Early Permian?||||||
27049|Mount Departure Microgranite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
27049|Mount Departure Microgranite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Microgranite and intrusive rhyolite; minor dacite.||||||19-AUG-04
27049|Mount Departure Microgranite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Porphyritic microgranite and intrusive rhyolite; minor porphyritic intrusive dacite.|
27049|Mount Departure Microgranite|68405|5|Briefly described|Map Legend|Permian|Permian|Unassigned. Early Permian? Kennedy Province?|||||Porphyritic microgranite and intrusive rhyolite; minor porphyritic intrusive dacite?|
27049|Mount Departure Microgranite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Porphyritic microgranite and intrusive rhyolite; minor porphyritic intrusive dacite.|
27049|Mount Departure Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned.|||||A-type. Porphyritic microgranite, rhyolite grading to microgranite, biotite granite.|
32039|Mount Dick beds|22482|5|Briefly described|p487||Middle Devonian|Of Capella Creek Group.||||||24-NOV-08
32039|Mount Dick beds|24491|4|Described|p15|||Of Capella Creek Group. Overlain by Mount Warner Volcanics.||||||
32039|Mount Dick beds|24615|5|Briefly described|CD|Middle Devonian||[Dcd].  Max. age possibly Early Devonian?  Siltstone with minor rhyolitic voclaniclastic sandstone.||||||
32039|Mount Dick beds|50208|5|Briefly described|Map Legend|Devonian|Devonian|Of the Capella Creek Group.||||||
32039|Mount Dick beds|50317|5|Briefly described|Map Legend|Devonian|Devonian|Of the Capella Creek Group.  Siltstone with minor rhylitic volcaniclastic sandstone; jasper.||||||09-JUN-04
32039|Mount Dick beds|61147|5|Briefly described|p377, p379. |||||Unit in Capella Creek Group.||Intruded by Mount Morgan trondhjemite and Bouldercombe Complex. Underlies the Mount Warner Volcanics.|Interbedded andesitic to dacitic lavas and sediments, with minor jasperoid and manganiferous sediments.|
32039|Mount Dick beds|61730|5|Briefly described|p1000||Silurian|Base of Capella Creek Group. Consists mainly of siltstone with minor volcaniclastic sandstone, basaltic to dacitic lavas and rare calcareous skarns. Geological Province: Yarrol Province.||||||
32039|Mount Dick beds|61808|5|Briefly described|p446|Middle Devonian|Early Devonian|Mount is Mt in text. Of Capella Creek Group.||||||
32039|Mount Dick beds|68008|3|Fully described|p144, p182, p579|Middle Devonian|Middle Devonian|Messenger and Taube (1994). Originally the basal part of the sequence named the Capella Creek beds (Kirkegaard et al., 1970). A 13 x 4 km belt of rocks along the Dee Range. Named after a peak S of Station Creek. No type section; two representative stratigraphic columns shown in Messenger and Taube (1994). Poor outcrops; strongly hornfelsed. A type area is a track up a spur, east of Mount Dick, beginning at GR248500 7378450 on the Bajool 100k sheet. Forms the steep eastern escarpment of the Dee Range; rugged topography and deeply incised creeks. c.500-600m thick. Unfossiliferous.||Basal Capella Creek Group.||Is overlain conformably by Mount Warner Volcanics. Is intruded by Bajool Quartz Diorite.|Fine-grained, sparsely feldspar- and quartz-phyric dacites, local hyaloclastites; siltstone, many silicified, minor sandstone, basaltic to dacitic lava; rare skarns.|
32039|Mount Dick beds|68679|5|Briefly described|p315|||Messenger and Taube (1994). Originally the basal part of the Capella Creek beds. Forms a belt 13km long and up to 4km wide along the Dee Range, SE from Station Creek. 500-600m thick. Similar island arc environment to overlying unit.||Capella Creek Group.||Is overlain by Mount Warner Volcanics. Is intruded by Bajool Quartz Diorite.|Mainly siltstone and fine sandstone, with lesser dacite lava that has sparse quartz and feldspar phenocrysts and locally hyaloclastite; strongly hornfelsed by Bajool Quartz Diorite.|
24396|Mount Dore Granite|22465|6|Mentioned|p934|||||||||
24396|Mount Dore Granite|22515|4|Described|Fig1p398,404,406||Paleoproterozoic|||||||07-NOV-08
24396|Mount Dore Granite|22667|6|Mentioned|Fig1 P234|||||||||
24396|Mount Dore Granite|23064|6|Mentioned|136|||||||||
24396|Mount Dore Granite|23069|5|Briefly described|p775 (fig 1)|||||||||
24396|Mount Dore Granite|23471|5|Briefly described|p110 Fig 1|Calymmian|Calymmian|Age: 1516+/-10 Ma (U-PB SHRIMP). Geological Province: Mount Isa Block.||||||
24396|Mount Dore Granite|23967|6|Mentioned|p1331|||||||||
24396|Mount Dore Granite|23974|5|Briefly described|p1452 Fig. 2a|Proterozoic|Proterozoic|Geological Province: Selwyn Region.  Age: 1498Ma (Rb-Sr).||||||
24396|Mount Dore Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24396|Mount Dore Granite|24256|6|Mentioned|p48, p50 Fig.2|||Mount is Mt. in text. Geological Province: Mount Isa Block.||||||
24396|Mount Dore Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
24396|Mount Dore Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
24396|Mount Dore Granite|37862|4|Described|p589|||||||||
24396|Mount Dore Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24396|Mount Dore Granite|38658|6|Mentioned|p153|||||||||
24396|Mount Dore Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24396|Mount Dore Granite|39445|6|Mentioned|Table 2|||||||||
24396|Mount Dore Granite|40840|6|Mentioned|Map legend|||||||||
24396|Mount Dore Granite|41306|6|Mentioned|p4|||||||||
24396|Mount Dore Granite|41979|6|Mentioned|p532|||||||||
24396|Mount Dore Granite|43490|6|Mentioned|8|||Of Narraku Batholith.||||||01-FEB-07
24396|Mount Dore Granite|43767|6|Mentioned|Fig.1,p890|||||||||
24396|Mount Dore Granite|45161|5|Briefly described|p52|||||||||
24396|Mount Dore Granite|45166|5|Briefly described|p39|||||||||
24396|Mount Dore Granite|49009|2|Defined|p27|Proterozoic|Proterozoic|Mapped as William Granite by Carter & Opik (1963).||||||
24396|Mount Dore Granite|49041|5|Briefly described|Table 3|||||||||
24396|Mount Dore Granite|50100|5|Briefly described|p13 Fig.4, p21|Calymmian|Calymmian|Of the Williams Supersuite. See also p61.||||||
24396|Mount Dore Granite|50536|5|Briefly described|p1.5, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite. Age: 1509 +/- 22Ma (Rb-Sr).||||||
24396|Mount Dore Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
24396|Mount Dore Granite|60658|6|Mentioned|p61|||Granite pluton. Mount is Mt in text. Geological Province: Eastern Fold Belt / Mount Isa Inlier||||||01-FEB-07
24396|Mount Dore Granite|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Pluton of the Williams and Naraku Batholiths. Age:1516-1490 Ma.||||||
24396|Mount Dore Granite|62047|6|Mentioned|p90 Fig.1  |||||||||
24396|Mount Dore Granite|64250|6|Mentioned|p11 fig 3, p15||||1516 +/- 10 Ma|||||
24396|Mount Dore Granite|65396|6|Mentioned|p7, p40, p53, p61, p82, p84, p157, p175|Calymmian|Calymmian|See also p182, p241, p327, p360-361, p438, p440, p445, p474-500. Kalkadoon-Leichhardt Belt. Stress partitioning and fluid flow models detailed.|1516 +/- 10 Ma|||||
24396|Mount Dore Granite|66913|5|Briefly described|p169, p170 fig 1, p171, p173, p179, 187|Calymmian|Calymmian|U-Pb zircon SHRIMP age shown diagramatically on Fig. 2.|~1500Ma|||||
24396|Mount Dore Granite|67323|4|Described|GIS attrib tbl, Solid Geology Map, p19|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. East of Selwyn, Kuridala-Selwyn Domain. Williams Igneous Event. Higher magnetic response.|1516 +/- 10 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.||Intrudes and is thrust over the Kuridala Group.|Non-porphyritic hornblende-biotite and biotite granite, minor aplite.|
24396|Mount Dore Granite|67498|5|Briefly described|p918 Fig. 1, p919, p928, p934|Calymmian|Calymmian|Defined by Blake (1987). High potassic granite. Dated by Pollard & McNaughton (1997).|1516 +/- 10 Ma.|Of the Williams-Naraku Suite.|||Non-foliated, partly porphyritic, biotite and hornblende-biotite granite with minor microgranites, aplites and pegmatites.|08-MAY-12
24396|Mount Dore Granite|68542|6|Mentioned|p17 fig 5, p18|||||||||
24396|Mount Dore Granite|68576|5|Briefly described|Q_2: p16-18|Proterozoic|Proterozoic|An intrusive phase of the 1545-1500 Ma Williams/Naraku Batholith, S of Cloncurry.||||||
24396|Mount Dore Granite|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Equigranular hornblende-biotite and biotite granite, minor aplite|
24396|Mount Dore Granite|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Equigranular hornblende-biotite and biotite granite, minor aplite|
24396|Mount Dore Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Non-porphyritic hornblende-biotite and biotite granite; minor aplite.|
24396|Mount Dore Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular hornblende-biotite and biotite granite; minor aplite.|20-JAN-22
24396|Mount Dore Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular hornblende-biotite and biotite granite; minor aplite.
|
24396|Mount Dore Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1516+/-10 Ma (U-Pb zircon SHRIMP)||||Granite.|
24396|Mount Dore Granite|72889|6|Mentioned|p8.|||||||||
24396|Mount Dore Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1516 +/- 10 Ma|||||
24396|Mount Dore Granite|73525|5|Briefly described|p4-5 Fig.2|Calymmian|Calymmian|Written as Mt Dore.|1510+/-10 Ma crystallisation age||||Felsic intrusive.|
23817|Mount Douglas Formation|23422|5|Briefly described|p180, p205 Table 6.3|Carboniferous|Early Carboniferous|Of Glenrock Group.||||||
23817|Mount Douglas Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group.||||||
23817|Mount Douglas Formation|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
23817|Mount Douglas Formation|24613|2|Defined|p9 Fig. 4, p96-97|Visean|Visean|Of Glenrock Gp. Formerly Plumtree Fm (unpub). Conform.on Percy Creek Volcs; conform.below Horse Pocket Volcs. Max.thick:1310m.Geol.prov: Burdekin Basin.Conglom., pebbly sst, volcanolithic sst, tuffaceous siltst, rhyolitic ignimbrite+crystal vitric tuffs||||||07-FEB-11
23817|Mount Douglas Formation|37573|4|Described|p225|||See also Fig.22||||||
23817|Mount Douglas Formation|38658|6|Mentioned|p152|||||||||
23817|Mount Douglas Formation|39445|5|Briefly described|p90|||See also Table 7||||||
23817|Mount Douglas Formation|39686|6|Mentioned|p73|||||||||
23817|Mount Douglas Formation|41774|6|Mentioned|p32|||||||||
23817|Mount Douglas Formation|42547|5|Briefly described|p76|||||||||
23817|Mount Douglas Formation|43095|6|Mentioned|p28|||of Glenrock Group?||||||
23817|Mount Douglas Formation|43933|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||
23817|Mount Douglas Formation|43935|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||22-FEB-05
23817|Mount Douglas Formation|68731|6|Mentioned|p187|||< 1313 m thick. Lower succession contains sporadic lepidodendroid plant remains.||||Conformably overlain by the Horse Pocket Volcanics.|Comprises crystal to vitric silicic tuff and tuffaceous siltstone; medium to coarse volcaniclastic sandstone; pebble to cobble polymict conglomerate; crystal vitric tuff and ignimbrite; tuffaceous claystone, siltstone and very fine sandstone.|
68997|Mount Eagle Volcanics|61087|5|Briefly described|Map Legend|Triassic|Triassic|Pink to orange, crystal rich, moderatly lithic-rich rhyolitic tuff, crystal-rich, fiamme-rich, mostly rhyolitic ignimbrite, flow-banded porphyritic rhyolite and breccia.||||||
68997|Mount Eagle Volcanics|64399|5|Briefly described|Map legend|Triassic|Triassic|Pink to orange, crystal-rcih, moderately lithic-rich rhyolitic tuff, crystal-rcih, flamme-rich, mostly rhyolitic ignimbrite, flwo-babded porphyritic rhyolite and breccia.||||||18-AUG-08
68997|Mount Eagle Volcanics|65388|1|Redefined|p203-206, p204, 205, 303, 304, 313, 314|Late Triassic|Late Triassic|Named and defined by Whitaker & others (1974) as Mount Eagle beds, for volcanic and sedimentary rocks exposed west of the Burnett River between Yards Gully and Smalls Creek, 18km north-west of Eidsvold. The name is herein changed to Mount Eagle Volcanics. Type locality at Wuruma Dam. Overlie granites of the late Permian to Early Triassic Rawbelle Batholith. Age from correlation with Aranbanga Volcanic Group to the south east. See also p318, 328.||||||
68997|Mount Eagle Volcanics|65452|6|Mentioned|p4 Fig.1|Late Triassic|Late Triassic|||||||
68997|Mount Eagle Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
68997|Mount Eagle Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
68997|Mount Eagle Volcanics|68679|5|Briefly described|p312-313, p353, p418-419, p429,p434,p441|Late Triassic|Late Triassic|Crops out west of Eidsvold, northern New England Orogen. Age based on lithological and stratigraphic similarity with the Aranbanga Volcanic Group. Dykes intruding this unit are associated with gold-bearing, epithermal, colloform and chalcedonic quartz veins and breccias.||||Overlies Culcraigie Granite; Euroka, Greystone Granodiorites. May intrude Morrow Granite. Adjacent to Boolgal Granophyre.|Lithic-rich, strongly welded dacitic ignimbrite; crystal-poor and intensely welded rhyolitic ignimbrite with spectacular rheomorphic foliation; rhyolitic to dacitic coherent lavas and associated autobreccias; minor volcaniclastic sandstone.|
68997|Mount Eagle Volcanics|73450|4|Described|p12, p26, p28|late Triassic|late Triassic|Complex arrangement of rhyolitic lavas and rhyolitic ignimbrites and breccias cropping out in undulating terrain northwest of Eidsvold. Probably correlated to Arangbanga [Volcanic Group] and Winterbourne Volcanics. Probably intruded by Boolgal Granophyre.|||||Rhyolite lavas, including very extensive autoclastic domains, and rhyolitic ignimbrites that are locally intensely welded/rheomorphic.|
72736|Mount Elmo Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
72736|Mount Elmo Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink, medium to coarse-grained equigranular biotite monzogranite.|
72736|Mount Elmo Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pink, medium to coarse-grained equigranular biotite monzogranite.|
72736|Mount Elmo Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, medium- to coarse-grained, equigranular biotite monzogranite; weakly foliated; granophyric.|
72736|Mount Elmo Granite|73450|6|Mentioned|p16|||||||||
29478|Mount Elvan Granite|23049|3|Fully described|p59|Devonian|Silurian|||||||
29478|Mount Elvan Granite|23283|2|Defined|p25|Devonian|Silurian|||||||
29478|Mount Elvan Granite|23422|5|Briefly described|p216 Table 6.10|||||||||
29478|Mount Elvan Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|||||||
36305|Mount Emu Rhyolite|23291|4|Described|p42, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Parent: Silent Creek Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
36305|Mount Emu Rhyolite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
24398|Mount Erle Igneous Complex|22522|6|Mentioned|p335|||||||||
24398|Mount Erle Igneous Complex|24197|5|Briefly described|p32, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24398|Mount Erle Igneous Complex|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24398|Mount Erle Igneous Complex|37862|4|Described|p585|||||||||
24398|Mount Erle Igneous Complex|38310|6|Mentioned|p237|||||||||
24398|Mount Erle Igneous Complex|38350|4|Described|p18|||||||||
24398|Mount Erle Igneous Complex|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24398|Mount Erle Igneous Complex|40840|6|Mentioned|Map legend|||||||||
24398|Mount Erle Igneous Complex|41272|6|Mentioned|M 1of1 D07|||||||||
24398|Mount Erle Igneous Complex|42879|6|Mentioned|p214|||Mount is Mt in text.||||||01-FEB-07
24398|Mount Erle Igneous Complex|45161|4|Described|p31|||||||||
24398|Mount Erle Igneous Complex|45166|5|Briefly described|p34|||||||||
24398|Mount Erle Igneous Complex|46976|6|Mentioned|Fig.1|||||||||
24398|Mount Erle Igneous Complex|49009|2|Defined|p28|Proterozoic|Proterozoic|||||||
24398|Mount Erle Igneous Complex|49041|5|Briefly described|Table 2|||||||||
24398|Mount Erle Igneous Complex|50100|5|Briefly described|p18, p55|Proterozoic|Proterozoic|Of the Burstall Suite (Wonga Batholith).  Granite, metadolerite and amphibolite of this complex host the Duchess orebody. Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||
24398|Mount Erle Igneous Complex|50536|5|Briefly described|p1.4, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||07-NOV-08
24398|Mount Erle Igneous Complex|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Leucocratic granite, dolerite, pegmatite.||||||
24398|Mount Erle Igneous Complex|65396|6|Mentioned|p319|||Mount Isa Inlier.|c.1740 Ma.|||||
24398|Mount Erle Igneous Complex|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Fine to medium-grained leucogranite; some dolerite and hybrid rocks.|
24398|Mount Erle Igneous Complex|67497|5|Briefly described|p889, p900 Tb.7,p909,  p911 Fig.20|Statherian|Statherian|Age from sample FBMI-5601.|1718 +/- 6 Ma U/Pb SHRIMP zircon.|Of the Burstall Suite.|||A-type granite spatially associated with minor Au-Cu mineralisation and possibly the product of relatively fractionated, late-stage melts of the Burstall magmatic event.|07-MAY-12
24398|Mount Erle Igneous Complex|69591|5|Briefly described|p60|||||Burstall Suite.|||Fine- to medium-grained leucogranite; some dolerite and hybrid rocks.|
24398|Mount Erle Igneous Complex|72596|5|Briefly described|p1-3, p23-24, p39-43, p45-48|Statherian|Statherian|Geochronologic constraint is a magmatic crystallisation age for this sample. Previous U-Pb zircon (SHRIMP) age of 1718+/- 6 Ma by Bierlein et al. (2011) interpreted to represent a relatively young (unmapped) phase that may correlate with granite of the Myubee Igneous Complex.Two titanate ages; a dominant group at 1500 +/- 6 Ma from 22 constituent analyses and another at 1556 +/- 18 Ma. These represent metamorphic events and are similar to metamorphic zircon ages elsewhere. The inferred metamorphic ages coincide with the emplacement ages for granitoids of the Williams and Naraku Batholiths. Correlated with / compositionally similar to the granitic component of the Myubee Igneous Complex, and the Overlander, Revenue and Burstall granites (see Bultitude et al., 1982; Blake et al., 1984).|1735 +/- 3 Ma SHRIMP U-Pb|Burstall Suite||Intrudes the Corella Formation.|Commonly foliated pink granite, metadolerite, gabbro, and 'diorite' together with minor aplite and quartz-feldspar pegmatite. Granite and dolerite/gabbro are intimately mixed locally to form net-veined complexes. (Blake et al., 1984).|
24398|Mount Erle Igneous Complex|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Leucogranite, minor aplite, pegmatite. Mixture of fine to medium-grained leucogranite, dolerite and dioritic hybrids; minor calc-silicate granofels enclaves. Fine to coarse-grained olivine-bearing dolerite. Graphic quartz-feldspar pegmatite.|
24398|Mount Erle Igneous Complex|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Leucogranite, minor aplite, pegmatite. Mixture of fine to medium-grained leucogranite, dolerite and dioritic hybrids; minor calc-silicate granofels enclaves. Fine to coarse-grained olivine-bearing dolerite. Graphic quartz-feldspar pegmatite.|
24398|Mount Erle Igneous Complex|72799|6|Mentioned|p1, p10, p19|Statherian|Statherian|Emplacement age of granite reported as 1735 +/- 3 Ma (Kositcin et al., 2019). Bierlein et al. (2011) reported slightly younger SHRIMP zircon emplacement ages (1718-1722 Ma) for parts of the unit suggesting it might be composite.|ca. 1735-1740 Ma, 1735 +/- 3 Ma|||Coeval with Myubee Igneous Complex.||
24398|Mount Erle Igneous Complex|73413|6|Mentioned|p8, App.1|Statherian|Statherian|U-Pb SHRIMP age of 1735 +/- 3 Ma and a metamorphic age of 1500 +/- 6 Ma was reported by Kositcin et al. (2019).|1735 +/- 3 Ma|||Intrudes the Corella Formation.|Includes granite.|
24398|Mount Erle Igneous Complex|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Mary Kathleen Domain.|1718+/-6 Ma crystallisation age||||Felsic intrusive.|
24398|Mount Erle Igneous Complex|73553|4|Described|p2-3, p8, p14, p43, p47, p59,|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Additional age 1500+/-6 Ma (titanite). Up to ~4 km wide with pronounced northerly elongation. Metamorphosed to amphibolite grade. May be a composite unit based on ages. Mainly mottled dark red-reddish brown tones on radiometric images,. Varied magnetic response from low to high (eastern part). See also p153, p155-156, p157-160, p162-p165, p173, p175-p178, p221, p250, p266.|1718+/-6 Ma and 1735+/-3 Ma U-Pb zircon (SHRIMP)|Burstall Suite||Intrudes Corella Formation|Consists mainly of granite with a steep northerly trending foliation, metadolerite grading into metagabbro and net-veined complexes of granite, metadolerite and 'dioritic hybrid rocks'. Minor pegmatite and aplite.|03-FEB-23
30005|Mount Finnigan Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30005|Mount Finnigan Granite|43070|2|Defined|p53|Late Permian||Of Cooktown Supersuite.||||||03-JUN-09
30005|Mount Finnigan Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic, cordierite(altered)-biotite granite.||||||06-JUL-04
30005|Mount Finnigan Granite|60425|5|Briefly described|p272 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite (no suite assigned). S-type. Massive, moderately to highly porphyritic, fine-grained cordierite (altered)-tourmaline-muscovite-biotite granite -- further lithological details included (p273).||||||07-FEB-11
30005|Mount Finnigan Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|||S-type granitoids.|
36713|Mount Formartine Suite|23423|5|Briefly described|311 Table 7.4p||Early Permian|S-type granite. Of Mount Formartine Supersuite||||||
77818|Mount Fort Bowen Sandstone|67323|5|Briefly described|GIS attrib tbl|Paleozoic|Proterozoic|Millungera Basin succession. Precambrian? - Paleozoic.|||||Red to purple, coarse- to very coarse-grained lithic sandstone and pebble to cobble conglomerate with abundant clasts of jasper and quartz; strongly cleaved at Mount Brown.|
77818|Mount Fort Bowen Sandstone|68146|5|Briefly described|p134-140|||An informal name, after Mount Fort Bowen.|1538 +/- 4 Ma; maximum depositional age.||||Purple, cross-bedded, coarse-grained sandstone with some heavy mineral bands. Overlies a clast-supported purple conglomerate interbedded with coarse-grained gritty sandstone. Unclear if this latter unit is included in this Formation.|
77818|Mount Fort Bowen Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|Millungera Basin.||||||
77818|Mount Fort Bowen Sandstone|69591|6|Mentioned|p29|Paleozoic|Neoproterozoic|||||||
77818|Mount Fort Bowen Sandstone|71592|5|Briefly described|Appendix A.|||Millungera Basin.|1538+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
77818|Mount Fort Bowen Sandstone|72889|6|Mentioned|p6 Fig.i.|||||||||
31420|Mount Fort Constantine Volcanics|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
31420|Mount Fort Constantine Volcanics|50332|6|Mentioned|p16, p62|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma.||||||07-FEB-11
31420|Mount Fort Constantine Volcanics|61936|5|Briefly described|p195 Fig. 6|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. Mount is Mt in text of figure. ||||||
31420|Mount Fort Constantine Volcanics|64248|5|Briefly described|p33 Fig.1, p36, p38 Fig.5, p39 |Statherian|Statherian|See also p40 Fig.6, p43 Fig.11.|1746 +/- 9 Ma and 1742 +/- 6 Ma.|||||
31420|Mount Fort Constantine Volcanics|64250|5|Briefly described|p10 fig 2, p23 fig 8, p11 fig 3, p21|||Cloncurry Fold Belt, Mount Isa Inlier. The Mount is omitted on p19. Overlaps or closely follows emplacement of Wonga batholith. May be shallow intrusions into Corella Formation.|1746+/-9 Ma; 1742+/-6 Ma.||||Felsic eruptions (or shallow intrusions).|
31420|Mount Fort Constantine Volcanics|64251|6|Mentioned|p51 Fig. 1|||Mount is Mt in figure. Geological Province: Mount Isa Inlier.||||||05-MAY-09
31420|Mount Fort Constantine Volcanics|65396|5|Briefly described|p4, p7, p16-17, p23, p78,p82, p173 Fig.2|Statherian|Statherian|See also p175, p179, p183, p187, p190, p192-193, p199, p213, p217, p222, p234-241, p272, p439. Eastern succession, Cover Sequence 2. Cloncurry Fold Belt. Abbreviated to Fort Constantine Volcanics on p201.|1746 +/- 9 Ma, 1742 +/- 6 Ma|||Cuts the Corella Formation.|Felsic volcanics (eruptions or shallow intrusions).|
31420|Mount Fort Constantine Volcanics|65755|6|Mentioned|p3 Fig.1|||Written Mt in text.||||||10-SEP-14
31420|Mount Fort Constantine Volcanics|67323|5|Briefly described|GIS attrib tbl, p17, p24, p32, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Canobie Domain, Mount Isa Inlier. Wonga/Burstall volcanic equivalents; may be comagmatic with Levian and Dipvale Granites. Highly magnetic. Occurs as numerous isolated outcrops; hosts the Ernest Henry mineralisation. Geochronology by Page and Sun (1998). May be the upper part of Corella Formation.|1746 +/- 9 Ma and 1742 +/- 6 Ma.|||(Interpreted to) overlie Corella Formation.|High-level intrusives and extrusives; brecciated felsic to intermediate volcanic rocks.|
31420|Mount Fort Constantine Volcanics|69056|4|Described|p2-6, p13, p18, p23, p28, p53-54|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Geological Survey of Queensland (2011). Constantine Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area. May be associated with the ~1740 Ma Wonga Event. Hosts the Ernest Henry deposit. Modelling values listed.|1746+/-9 Ma - 1742+/-6 Ma (Page and Sun, 1998).|||Overlies Corella Formation.|Brecciated felsic to intermediate volcanics.|
31420|Mount Fort Constantine Volcanics|69591|5|Briefly described|p33, p36, p56, p105|||Canobie Domain, Leichhardt Superbasin. Forms several isolated outcrops. Hosts mineralisation at the Ernest Henry mine. Continues to the N under cover. Associated with the Wonga Extension Event. Ages by Page and Sun (1998).|1746 +/- 9 Ma; 1742 +/- 6 Ma.|||Overlies (?forms part of) Corella Formation.|Brecciated felsic to intermediate volcanic rocks.|
31420|Mount Fort Constantine Volcanics|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Brecciated felsic to intermediate volcanic rocks.|
31420|Mount Fort Constantine Volcanics|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Brecciated felsic to intermediate volcanic rocks.|
31420|Mount Fort Constantine Volcanics|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Brecciated felsic to intermediate volcanic rocks.|
31420|Mount Fort Constantine Volcanics|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Brecciated felsic-intermedite volcanic rocks.|
31420|Mount Fort Constantine Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen. Both age determinatons are titanite U-Pb SHRIMP.|1529+/-11 Ma and 1514+/-24 Ma.|||||
31420|Mount Fort Constantine Volcanics|72596|5|Briefly described|p9-10, p24|Statherian|Statherian|Geochronologic constraint from Page and Sun (1998). Several isolated outcrops near the Ernest Henry mine northeast of Cloncurry.|1746 +/- 9 Ma and 1742 +/- 6 Ma|||May either overlie or form the upper part of the Corella Formation.|Felsic to intermediate volcanics.|
31420|Mount Fort Constantine Volcanics|73137|6|Mentioned|p2, p39, p51, p68, p72|Statherian|Statherian|Extrusive igneous rocks associated with volcanic rocks of the Corella Formation.|[c. 1737 Ma]|||Coeval with Corella Formation.||
31420|Mount Fort Constantine Volcanics|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
31420|Mount Fort Constantine Volcanics|73529|6|Mentioned|p15 Fig.11|Statherian|Statherian||1750-1710 Ma|||||
26761|Mount Frosty Member|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Argylla Formation.  Feldspathic sandstone and conglomerate.||||||09-FEB-09
77804|Mount Garling Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Grey to pink, medium grained, porphyritic biotite granite with K-feldspar phenocrysts > 2 cm and clots of biotite.|
28797|Mount Gillies Rhyolite|30604|6|Mentioned|p66|||||||||
28797|Mount Gillies Rhyolite|32924|6|Mentioned|p111|||Replaces Mt. Lindesay & Hillview Rhyolites||||||
28797|Mount Gillies Rhyolite|36806|6|Mentioned|p131|||||||||
28797|Mount Gillies Rhyolite|39445|5|Briefly described|Table 14|||||||||
28797|Mount Gillies Rhyolite|40587|6|Mentioned|p361|||||||||
28797|Mount Gillies Rhyolite|40623|5|Briefly described|p39|||Formerly Hillview Rhyolite||||||
28797|Mount Gillies Rhyolite|40780|5|Briefly described|p9|||||||||
28797|Mount Gillies Rhyolite|40896|6|Mentioned|p4|||||||||
28797|Mount Gillies Rhyolite|69599|5|Briefly described|p595, p631, p640|Miocene|Miocene|Main Range. Table of chemical analyses. Formerly the Hillview Rhyolite and Mount Lindesay Rhyolite. Appears as Mount Gilles Rhyolite on p631.||||Is overlain by the Chinghee Conglomerate.||
28797|Mount Gillies Rhyolite|73450|4|Described|p96-98|Chattian|Chattian|Associated with the Focal Peak volcano. Comprises lava flows with some intrusive components. Thickest flows occur at Mount Lindesay where two flows comprise 180 m of rhyolite lava overlying 60 m of rhyolitic agglomerate and fine-grained, banded rhyolitic tuff. Autobreccia is locally common. Yielded K-Ar ages of 24.8 +/- 0.2 Ma and 25.5 +/- 0.2 Ma (Ewart, 1982) and 23.3 Ma and 23.3 Ma (Webb, 1967).|ca 25 Ma|||Overlain by Chinghee Conglomerate.|Dominated by rhyolitic lava close to the vent and pyroclastic ashfall tuffs agglomerates and boulder deposits in more distal regions.|
22420|Mount Glengalder Granite|23049|3|Fully described|p8|Ordovician|Ordovician|Age: Middle Ordovician.||||||
22420|Mount Glengalder Granite|23283|2|Defined|p25|Devonian|Silurian|||||||
80724|Mount Glenroy microgranite|71031|5|Briefly described|p3, p44, p50|Permian|Ordovician|Charters Towers Province. Inferred as the source of Mo-W quartz veins and Au-base metal mineralisation at Mount Glenroy.||||Intrudes the Mount Windsor Volcanics (age:481.5 +/-2.7Ma).||28-FEB-19
22421|Mount Grey Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 136. I-Type.||||||
22421|Mount Grey Granite|23617|4|Described|p18 Table 2|||I-Type. Also see p31. Intrudes Kangaroo Hills Formation. Table 3 p52. Kennedy Province.||||||
22421|Mount Grey Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
22421|Mount Grey Granite|43259|4|Described|Appendix 1,p25.||Carboniferous|||||||
22421|Mount Grey Granite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
25279|Mount Hall Formation|22675|5|Briefly described|p34|||Drummond Basin||||||
25279|Mount Hall Formation|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
25279|Mount Hall Formation|23161|4|Described|p13 table2b|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|23430|5|Briefly described|p510|||Drummond Basin Province||||||
25279|Mount Hall Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Quartzose sandstone and conglomerate; minor lithic sandstone and mudstone.  Max. thickness: 1200m.  Geological Province: Drummond Basin.||||||
25279|Mount Hall Formation|30151|6|Mentioned|p13|||Upper Devonian?-Lower Carboniferous age. See also Fig.3||||||
25279|Mount Hall Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
25279|Mount Hall Formation|31984|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|32490|4|Described|Table 1|||||||||
25279|Mount Hall Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|32553|4|Described|p46|||||||||
25279|Mount Hall Formation|32556|4|Described|Table 2|||L.Carb.||||||
25279|Mount Hall Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|33645|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25279|Mount Hall Formation|33646|6|Mentioned|p18|||Hydrology.||||||
25279|Mount Hall Formation|34389|4|Described|Table 1|||Lower Carboniferous||||||
25279|Mount Hall Formation|34390|4|Described|Table 1|||Upper Devonian||||||
25279|Mount Hall Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|34392|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|35811|5|Briefly described|Table 4|||||||||
25279|Mount Hall Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25279|Mount Hall Formation|37451|6|Mentioned|Table 2|||||||||
25279|Mount Hall Formation|37573|4|Described|Table 2|||||||||
25279|Mount Hall Formation|39445|5|Briefly described|Table 6|||||||||
25279|Mount Hall Formation|40623|5|Briefly described|p110|||||||||
25279|Mount Hall Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
25279|Mount Hall Formation|41710|5|Briefly described|p226|||||||||
25279|Mount Hall Formation|41805|6|Mentioned|Fig.2|||||||||
25279|Mount Hall Formation|42486|5|Briefly described|p201|||||||||
25279|Mount Hall Formation|42547|5|Briefly described|Fig.17 P61|||||||||
25279|Mount Hall Formation|42614|4|Described|p9|||Drummond Basin||||||
25279|Mount Hall Formation|42701|3|Fully described|p25|||||||||
25279|Mount Hall Formation|43029|5|Briefly described|p24|||||||||
25279|Mount Hall Formation|43105|6|Mentioned|p12|||||||||
25279|Mount Hall Formation|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||underlies Raymond Sandstone, overlies Telemon Formation||23-DEC-11
25279|Mount Hall Formation|43213|4|Described|p90, p92, p94, p238|||Drummond Basin. Originally named Mount Hall Conglomerate by Shell (Queensland) Development Pty Ltd (1954), and others. Part of Olgers (1972) non-volcanic Cycle 2. Forms steep strike ridges. 3000m thick, thinning rapidly to the S. Geophysics described.|||||Conglomerate with clasts of milky quartz in a matrix of poorly sorted sandstone, with grey quartz sandstone and pebbly quartz sandstone in well-defined beds separated by thick beds of olive-green mudstone and lithic and feldspathic quartz sandstone.|
25279|Mount Hall Formation|44081|14|Not recorded|Fig.8,Pl.8|||||||||
25279|Mount Hall Formation|44098|14|Not recorded|p98|||||||||
25279|Mount Hall Formation|44245|5|Briefly described|Map Legend||Carboniferous|||||||
25279|Mount Hall Formation|44331|14|Not recorded|Map Legend||Early Carboniferous|||||||
25279|Mount Hall Formation|44573|14|Not recorded|p98|||||||||
25279|Mount Hall Formation|45073|3|Fully described|p27|||Marker||||||
25279|Mount Hall Formation|45151|5|Briefly described|Table 6|||||||||
25279|Mount Hall Formation|46849|6|Mentioned|Fig. 2|||||||||
25279|Mount Hall Formation|46881|6|Mentioned|Table 2|||||||||
25279|Mount Hall Formation|48914|5|Briefly described|p35|||Stratigraphy.||||||
25279|Mount Hall Formation|48922|4|Described|p12|||||||||
25279|Mount Hall Formation|48951|6|Mentioned|Table 1|||||||||
25279|Mount Hall Formation|60659|4|Described|p13-14|Early Carboniferous|Early Carboniferous|Grey quartz sandstone, pebbly quartz sst. Conglomerate, shale and siltstone. A marker unit in the basin. Overlies Silver Hills Volcanics and Anakie Metamorphic Group; overlapped by Raymond Formation. Geol Prov: Drummond Basin.||||||07-FEB-11
25279|Mount Hall Formation|64315|5|Briefly described|p510 Tb. 1|Early Carboniferous|Early Carboniferous|Max. thickness: 1200m. Geological province: southern Drummond Basin. Quartzose sandstone, conglomerate; minor lithic sandstone, mudstone. Mount is Mt in text. ||||||
25279|Mount Hall Formation|64849|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.||||||
25279|Mount Hall Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.||||||
25279|Mount Hall Formation|64852|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Quartzose to feldspathic sublabile sandstone, quartz pebble conglomerate, mudstone and red and green siltstone.||||||
25279|Mount Hall Formation|66085|5|Briefly described|Map legend|Carboniferous|Carboniferous|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone, red and green siltstone.||||||
25279|Mount Hall Formation|66188|6|Mentioned|Fig 3, Fig 16-17, TB1|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
25279|Mount Hall Formation|67402|4|Described|p165 tbl LPB1, p196 fig DRM2|Tournaisian|Tournaisian|Drummond Basin. Deposited in high-low energy fluvial environments. See also p197, p198 fig DRM3, p201 tbl DRM2.||||Overlies the Scartwater Formation. Overlain by the Raymond and Star of Hope Formations.|Quartz sandstone, pebble quartz sandstone, conglomerate, shale and siltstone.|
25279|Mount Hall Formation|68326|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Telemon Formation. Is overlain conformably by Raymond Sandstone.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|02-DEC-13
25279|Mount Hall Formation|68329|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Is overlain conformably by Star of Hope Formation.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68347|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Is overlain conformably by Star of Hope Formation.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68404|5|Briefly described|Map legend|Carboniferous|Carboniferous|Drummond Basin|||||Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68411|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||Shown as lateral equivalent of the Raymond Sandstone. Conformably overlain by the Star of Hope Formation. Conformably underlain by the Silver Hills Volcanics.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68412|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Is conformably overlain by Raymond Sandstone.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|23-JUN-15
25279|Mount Hall Formation|68413|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||Conformably overlain by the Raymond Sandstone.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68414|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin. Map symbol (Ch) indicates unit considered to be Carboniferous.||||Conformably overlain by the Star of Hope Formation. Conformably underlain by the Telemon Formation.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|29-AUG-14
25279|Mount Hall Formation|68423|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|Drummond Basin. This unit is incorrectly colour-coded in the "Palaeozoic Units" inset on the sheet.||||Is overlain conformably by Raymond Sandstone.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68482|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlain by the Raymond Sandstone. Conformably underlain by the Telemon Formation.|Quartzose to feldspathic sublabile sandstone, quartz-pebble conglomerate, mudstone and red and green siltstone.|
25279|Mount Hall Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Scartwater and Telemon Formations and Raymond Sandstone, are all mapped under the symbol, Cd2.||||||
25279|Mount Hall Formation|68731|5|Briefly described|p173 Fig 3.85, p191 Fig 3.102, p196|Mississippian|Mississippian|Drummond Basin. < 3000 m thick. Detailed lithology discussed. Contains rare occurrences of the Mississippian lycopod Lepidodendron veltheimianum (White cited in Olgers 1972).||||Conformably underlain by the Telemon Formation. Conformably overlain by the Raymond Formation.|Dominated by trough to planar cross-laminated, medium to coarse quartz sandstone, pebbly sandstone and minor quartz pebble conglomerate.|17-JUL-14
25279|Mount Hall Formation|68900|2|Defined|p4, p37, p52, p54-p55|Carboniferous|Carboniferous|Drummond Basin. Potentially not a true formation as the name has been applied to sand-dominated facies at different levels of the stratigraphy. Outcrops from the north of Drummond Basin to the very southern part of the Nogoa Anticline. Originally named the Mount Hall Conglomerate (SQD, 1952; Hill, 1957) but was renamed the Mount Hall Formation by Olgers (1972). The type locality is at Mount Hall in the Telemon Anticline in NANDOWRIE. This unit is resistive to weathering and forms high hills and prominent ridges. In airborne radiometrics this unit has a very low response and also a very low repsonse in magnetics. Interpreted to have been deposited in a meander belt and floodplain environment as part of a braided stream system. Olgers (1972) stated that the thickest part of the Mount Hall Formation is 3000m though it thins rapidly towards the margins. In Scartwater this unit is approx. 1000m thick and to the south of the basin it is between 300 and 750m thick. See also p57-p58, p62-p65, p70.||||Overlain by the Raymond Sandstone. Conformably overlain by the Star of Hope Formation. Conformably overlies the Scartwater Formation and Telemon Formation.|Fine- to very coarse-grained, well rounded, medium-thick bedded and cross-bedded sandstone and minor conglomerate.|
25279|Mount Hall Formation|70740|5|Briefly described|p42|||||||Overlies the Stones Creek Volcanics.||
25279|Mount Hall Formation|70856|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||Overlain conformably by Star of Hope Formation, conformably overlies Telemon Formation.|Quartzose to feldspathic sublabile sandstone, quartz pebble conglomerate, mudstone and green and red siltstone.|
25279|Mount Hall Formation|70857|5|Briefly described|Map Legend|Carboniferous|Devonian|||||Overlain by Star of Hope Formation, overlies Telemon Formation|Quartzose to feldspathic sublabile sandstone, quartz pebble conglomerate, mudstone and siltstone.|
25279|Mount Hall Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Early Carboniferous|Geological province: Drummond Basin.||||Overlain by Raymond Formation. Underlain by Scartwater Formation and Telemon Formation in the northern and southern parts of Drummond Basin respectively.||
25279|Mount Hall Formation|73198|4|Described|p498-501, p503-505, p507, p509-516|Visean|Visean|[Also written as Mt Hall Formation]. Drummond Basin. Part of Cycle 2 of Olgers (1972). Maximum thickness: 3000 m in the north (Olgers, 1972), thinning rapidly towards the basin margins (thickest measured section in this study is greater than 1082 m). Most distinctive and quartz-rich formation in the basin succession. Distinctive cross-stratified pebble conglomerate beds used as a valuable stratigraphic marker across the basin. Geochron is detrital zircon depositional age for upper part of the unit; corroborates biostratigraphic interpretation. Contains rare Lepidodendron and cordaitalean fossils in erosional bed bases. Fossilised wood and plant debris evident. Northerly to north-easterly directed paleocurrent indicators. Basement provenance. [See article for petrographic descriptions and data, and detailed conglomerate clast analysis].|ca 340 Ma|||Conformably underlain by Scartwater Formation and Telemon Formation. Conformably overlain by Raymond Formation.|Dominately quartzose conglomerate, pebble sandstone and sandstone including distinctive cross-stratified pebble conglomerate beds.|
30006|Mount Hartley Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30006|Mount Hartley Granite|43070|2|Defined|p60|||of Cooktown Supersuite. K-Ar age of 254+/-2Ma may be reset rather than crystallisation age.||||||
30006|Mount Hartley Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic biotite granite.||||||
30006|Mount Hartley Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Mount Hartley Suite (Cooktown Supersuite). S-type. Fine-gr., highly to slightly (locally) porphyritic, (altered cordierite-)tourmaline-biotite granite; extensively altered (greisenised) in places, with cassiterite deposits - more detail given.||||||07-FEB-11
30006|Mount Hartley Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Hartley Suite.|||S-type granitoids.|
36720|Mount Hartley Suite|23423|5|Briefly described|Table 7.1 p240|||Of Cooktown Group.||||||
36720|Mount Hartley Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains Mount Hartley Granite and Mount Leswell Microgranite. S-type.||||||07-FEB-11
36720|Mount Hartley Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Mount Hartley Granite, Mount Leswell Microgranite.||S-type granitoids.|
75645|Mount Hector Granite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Pale grey, fine to medium-grained, slightly porphyritic, granophyric hornblende-biotite monzogranite to granodiorite?; traces of titanite and allanite, and scattered mafic inclusions up to c. 3 cm across; deformed and partly recrystallised.|
26315|Mount Helpman Member|23291|4|Described|86 Tb. 3.6p|||Parent: Robertson River Subgroup. Geological Province: Georgetown Region.||||||26-MAY-15
26315|Mount Helpman Member|38714|2|Defined|p186|Mesoproterozoic|Mesoproterozoic|||||||
26315|Mount Helpman Member|39495|6|Mentioned|p142|||||||||
26315|Mount Helpman Member|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob. Early Proterozoic||||||26-MAY-15
26315|Mount Helpman Member|41272|6|Mentioned|M 1of1 L04|||||||||
26315|Mount Helpman Member|41975|5|Briefly described|Table 1 P434|||||||||
26315|Mount Helpman Member|43664|4|Described|p23-25|||||||||
26315|Mount Helpman Member|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Daniel Creek Formation (Robertson River Subgroup).||||||07-NOV-08
26315|Mount Helpman Member|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||30-JUL-04
26315|Mount Helpman Member|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Daniel Creek Formation.|||Mica schist, abundant quartzite and some calc-silicate rocks; abundant muscovite granite and pegmatite dykes and small stocks.|
26315|Mount Helpman Member|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1770 Ma (MDA: U-Pb zircon SHRIMP)||||Micaceous quartzite schist.|
24400|Mount Hogan Granite|22669|6|Mentioned|P250||Mesoproterozoic|Mount actually spelt Mt in text.  Age of unit is 1549+/-25 Ma||||||16-JAN-07
24400|Mount Hogan Granite|23220|5|Briefly described|Fig.1,2 p11||Mesoproterozoic|Age: U/Pb zircon SHRIMP 1549+/-25Ma. In the Forsayth Subprovince.||||||16-JAN-07
24400|Mount Hogan Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Geological Province: Georgetown Region.||||||18-JUN-15
24400|Mount Hogan Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 822. S-Type.||||||
24400|Mount Hogan Granite|24197|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Forsayth Supersuite. Geological province: Georgetown Inlier.||||||07-FEB-11
24400|Mount Hogan Granite|35920|2|Defined|p25|Neoproterozoic|Neoproterozoic|Prob.Late Proterozoic||||||
24400|Mount Hogan Granite|36937|6|Mentioned|p229|||||||||
24400|Mount Hogan Granite|37570|4|Described|p121|||||||||
24400|Mount Hogan Granite|37573|6|Mentioned|Fig.12|||||||||
24400|Mount Hogan Granite|37576|5|Briefly described|p8|||||||||
24400|Mount Hogan Granite|37614|6|Mentioned|p233|||||||||
24400|Mount Hogan Granite|39445|5|Briefly described|Table 2|||See also p72 and p148.  Formerly part of Robin Hood Granodiorite.||||||16-JAN-07
24400|Mount Hogan Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24400|Mount Hogan Granite|41272|5|Briefly described|M 1of1 B06|||||||||
24400|Mount Hogan Granite|43103|6|Mentioned|p16|||||||||
24400|Mount Hogan Granite|43259|4|Described|Appendix 1,p54.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
24400|Mount Hogan Granite|43664|6|Mentioned|p80|||||||||
24400|Mount Hogan Granite|43793|5|Briefly described|p333|||U-Pb age: 1549+/-25 Ma||||||
24400|Mount Hogan Granite|50211|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1550-1560 Ma.||||||17-MAY-04
24400|Mount Hogan Granite|50537|5|Briefly described|p1.2, 1.4, 2.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.  Age: 1549 +/- 25Ma (U-Pb).||||||
24400|Mount Hogan Granite|61258|6|Mentioned|p389|Mesoproterozoic|Mesoproterozoic|Age: 1549+/-25Ma (Black and Withnall 1993). Mount is Mt in text.||||||
24400|Mount Hogan Granite|63866|4|Described|p77|Calymmian|Calymmian|Numeric age is a U-Pb zircon TIMS date.|1549 +/- 25 Ma (Black, OZCHRON)|Forsayth Supersuite|||Medium- to coarse-grained biotite granite.|
24400|Mount Hogan Granite|66529|5|Briefly described|p62|||Hosts Au-U deposit in sinusoidal quartz-sulfide veins in sericite-chlorite altered zones. Age of mineralisation probably Proterozoic.|c.1558 Ma (Kositcin, unpublished data).||||Biotite granite.|
24400|Mount Hogan Granite|66800|6|Mentioned|p926.||||1549 +/- 25 Ma (Black & Withnall 1993).|||||
24400|Mount Hogan Granite|67341|5|Briefly described|p46-48|Calymmian|Calymmian|Etheridge Province. Has a very high background gamma-ray spectrometric signature. Magmatic crystallisation age.|1558 +/- 2 Ma (SHRIMP U-Pb zircon).|Forsayth Supersuite.|||Includes pink-grey, coarse-grained biotite monzogranite.|
24400|Mount Hogan Granite|68357|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province. High K, Th and U radiometric responses.|||||Grey to reddish-brown, medium- to coarse-grained, sparsely porphyritic biotite granite; a less fractionated phase is mapped separately, as is a strongly sericitically altered and quartz-veined granite.|
24400|Mount Hogan Granite|69591|5|Briefly described|p81, p83|Mesoproterozoic|Mesoproterozoic|Gilberton area. Although not part of the Forsayth Batholith, this unit probably belongs in the Forsayth Supersuite. Has a strong radiometric signature, high in K, U and Th; hosts uranium deposits.|1558 +/- 2 Ma (Neumann and Kositcin, 2011).||||Generally pink to cream, equigranular, coarse-grained, biotite granite.|
24400|Mount Hogan Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1549+/-25 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
24400|Mount Hogan Granite|73642|5|Briefly described|p4 Tb.1, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier. Age of 1549+/-50 Ma from Black and Withnall (1993), revised by a later study.|1549+/-50 Ma|Forsayth Supersuite||||
24400|Mount Hogan Granite|75079|6|Mentioned|p3|||Northeast Queensland.||||||
32043|Mount Hoopbound Formation|22482|4|Described|p487, p490||Late Devonian|Formerly the Dee Volcanics and Boulder Creek Grit. See also Fig. 1||||||
32043|Mount Hoopbound Formation|23468|5|Briefly described|p 296|||spelt "Mt" in text||||||
32043|Mount Hoopbound Formation|23522|5|Briefly described|p250 Fig 6|Late Devonian|Middle Devonian|||||||
32043|Mount Hoopbound Formation|24399|5|Briefly described|p275, p272 Fig. 1|Late Devonian|Late Devonian|Mount is Mt. in text.  Volcaniclastic sediments, minor limestone, some primary volcanic rocks.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt. See also p282.||||||
32043|Mount Hoopbound Formation|24491|4|Described|p17|Late Devonian|Late Devonian|Supersedes Dee Volcanics and Boulder Creek Grit.||||||
32043|Mount Hoopbound Formation|24615|5|Briefly described|CD|Late Devonian|Late Devonian|[Dh].  Granule to boulder andesitic to dacitic volcaniclastic breccia and conglom., locally fossiliferous; lithic to feldspatholithic sst., porphyritic andesite, lapilli to ash tuff, tuffaceous sandstone; minor ignimbrite; rare hyaloclastite and limestone||||||
32043|Mount Hoopbound Formation|50197|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32043|Mount Hoopbound Formation|50208|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32043|Mount Hoopbound Formation|50215|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Granule to boulder andesitic to dacitic volcaniclastic breccia and conglomerate, locally fossiliferous - more lithology included.||||||18-JUN-09
32043|Mount Hoopbound Formation|50317|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32043|Mount Hoopbound Formation|60282|5|Briefly described|p9|Late Devonian|Late Devonian|Incorporates two previously separately mapped units, the Dee Volcanics and Boulder Creek Grit.  Geological Province: Yarrol Province.||||||
32043|Mount Hoopbound Formation|61035|6|Mentioned|p12|Early Carboniferous|Late Devonian|Geological Province: Yarrol Province.||||||07-FEB-11
32043|Mount Hoopbound Formation|61147|5|Briefly described|p376 Fig.1, p378,  p383. |Frasnian|Frasnian|Part equivalent to Dee Volcanics of Kirkegaard et al.(1970). Limestones span four conodont zones, equating with the last half of the Frasnian.||||Unconformably overlies the Mount Morgan Trondhjemite.||
32043|Mount Hoopbound Formation|61392|5|Briefly described|p165 Fig. 2|Famennian|Frasnian|Part of the 'Bindawallah Stratigraphic Assemblage'.||||||07-FEB-11
32043|Mount Hoopbound Formation|61730|5|Briefly described|p994 Fig.1, p1000 Fig.3|Early Carboniferous|Late Devonian|Dominant rock type is volcanic conglomerate with clasts of basaltic to andesitic composition; with coral and conodont faunas in limestone lenses, brachiopods in clastic rocks indicating a marine environment. Geol Prov: Yarrol Province. Mount is Mt in Text||||||
32043|Mount Hoopbound Formation|63600|5|Briefly described|p900 Fig. 1, p915|Early Carboniferous|Late Devonian|Part of the volcanic/sedimentary sequences unconformably overlying Capella Creek Group. Mount is Mt in text of figure.||||||07-FEB-11
32043|Mount Hoopbound Formation|65214|6|Mentioned|p282|Devonian|Devonian|QLD, Mount Morgan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
32043|Mount Hoopbound Formation|65388|6|Mentioned|p72, 92, 158|Late Devonian|Late Devonian|Yarrol Province. May correlate with Tanderra Volcanics. Also given as Hoopbound Formation.||||||
32043|Mount Hoopbound Formation|68008|2|Defined|p36, p39-40, p50-55, p58-65, p67, p69|Famennian|Frasnian|See also p71, p77, p79-80, p90, p131, p309, p313-314, p318, p320, p476-477, p488, p573, p578-581, p598. Originally mapped by Maxwell (1952, 1953). Kirkegaard et al. (1970) revised the stratigraphy into three units, two named: Dee Volcanics and Boulder Creek Grit. Randall (1996) and Yarrol Project Team (1997) combine these two, and most of the unnamed remainder, into the Mount Hoopbound Formation. Named after Mount Hoopbound, 15km SSE of Mount Morgan. Type section by Randall (1996) is along Raspberry Creek 1.5km S of Mount Hoopbound. Mature island-arc deposits. Lithology described and illustrated in great detail; composite stratigraphic sections. Geochemistry discussed. Island arc, partly emergent, setting. 1,000-1,100m thick. Coral species listed. Correlated with Channer Creek beds. At least partly equivalent to Balaclava Formation (and overlain by it), Lochenbar, Mount Alma Formations and Three Moon Conglomerate. Micropaleontology table. Appears as Hoopbound Formation on p602.||||Overlies Mount Morgan Trondhjemite nonconformably, Raspberry Creek Formation (Capella Creek Group) unconformably. Unconformably underlies Youlambie Conglomerate. Is intruded by Eulogie Park Gabbro.|Dominantly pebble to cobble andesitic breccia/conglomerate; also basal polymictic conglomerate, lithic sandstone, siltstone, lapilli tuff, ash tuff, andesite and basaltic lavas. Brecciation is common.|
32043|Mount Hoopbound Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Balaclava and Lochenbar Formations, the Tanderra Volcanics,  the Channer Creek beds and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
32043|Mount Hoopbound Formation|68679|5|Briefly described|p310, p312-313, p316, p337-339, p349|Famennian|Frasnian|See also p403, p468. Rockhampton Subprovince, Yarrol Province. West and south of Mount Morgan. Originally mapped as Dee Volcanics (Frasnian), Thomson Clastics (Frasnian) and Boulder Creek Grit (Famennian) by Maxwell (1952, 1953). Kirkegaard et al. (1970) incorporated the Thomson Clastics into the Boulder Creek Grit. Randall (1996) and the Yarrol Project Team (1997) combined the Dee Volcanics and Boulder Creek Grit, with other undifferentiated Late Devonian units, as the Mount Hoopbound Formation. Basalts are typical of mature island arcs. Shallow-marine to subaerial deposits.||||Unconformably overlies Ginger Creek Member (Raspberry Creek Formation). Overlies Mount Morgan Trondhjemite.|Mainly pebble to cobble andesitic breccia and conglomerate, with lithic sandstone, siltstone, silty to pebbly tuff and basaltic andesite lava. Thin rhyolite flows in middle and upper sections. Brecciation common. Local basal polymict conglomerate.|
32043|Mount Hoopbound Formation|70740|5|Briefly described|p49|||Yarrol Province. Incorporates rocks of the former Boulder Creek Grit. ||||Equivalent to the Mount Wyatt Formation.||
69647|Mount Hutton Volcanics|61155|5|Briefly described|p20|Late Oligocene|Early Oligocene|In the Rockhampton-Gladstone area.||||||
35603|Mount Jeffreys ignimbrite|23277|5|Briefly described|p64|||||||||
24401|Mount Juliet Granite|23291|4|Described|p89 Fig. 3.8|||Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||11-MAY-15
24401|Mount Juliet Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 57. Assumed to be I-Type.||||||
24401|Mount Juliet Granite|23619|4|Described|p40 Table 2|||Intrudes Einasleigh Metamorphics. Also see p7. Copperfield Batholith Province.||||||
24401|Mount Juliet Granite|39981|2|Defined|p104|Devonian|Middle Silurian|Middle Proterozoic||||||
24401|Mount Juliet Granite|40542|6|Mentioned|p98|||||||||
24401|Mount Juliet Granite|41680|3|Fully described|p121|||||||||
24401|Mount Juliet Granite|43113|4|Described|Table 2 p26|||Proterozoic or Silurian to Early Devonian.||||||
24401|Mount Juliet Granite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24401|Mount Juliet Granite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
24401|Mount Juliet Granite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
24401|Mount Juliet Granite|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Biotite-muscovite granite and granodiorite.||||||
24401|Mount Juliet Granite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Grey, medium- to coarse-grained biotite-muscovite granite and granodiorite.|
24401|Mount Juliet Granite|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Grey, medium to coarse-grained biotite-muscovite granite and granodiorite.|
24401|Mount Juliet Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
36507|Mount Kataughal complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 152.  I-Type.||||||
30001|Mount Leswell Microgranite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30001|Mount Leswell Microgranite|43070|2|Defined|p41||Late Permian|of Cooktown Supersuite.||||||
30001|Mount Leswell Microgranite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite.  Porphyritic biotite granite.||||||
30001|Mount Leswell Microgranite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Mount Hartley Suite (Cooktown Supersuite). S-type. Dark grey, fine-gr., slightly to moderately porphyritic biotite granite; accessory ilmenite, apatite, zircon, allanite, tourmaline, muscovite, cassiterite, fluorite; more lithological detail included.||||||07-FEB-11
30001|Mount Leswell Microgranite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Hartley Suite.|||S-type granitoids.|
36451|Mount Little Volcanic Group|23291|4|Described|p43, p94 Tb. 3.9|Early Permian|Early Permian|Informal name. Previously included in the former "Croydon Volcanics". Geological Province: Georgetown Region.||||||04-JUN-15
36451|Mount Little Volcanic Group|23430|5|Briefly described|p493|||Kidston Subprovince. Kennedy Province.||||||
36451|Mount Little Volcanic Group|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||Includes Little Pocket Dacite; McFarlanes and Goat Creek Andesites; Linley and Bullseye Rhyolites.|||
36451|Mount Little Volcanic Group|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||Includes Little Pocket Dacite; McFarlanes and Goat Creek Andesites; Linley and Bullseye Rhyolites.|||
36451|Mount Little Volcanic Group|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek and Galloway Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork, Mitchell River and Nychum Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
36451|Mount Little Volcanic Group|69593|5|Briefly described|p490|Permian|Permian|Kidston Subprovince, Kennedy Igneous Association. Unassigned. Includes M-types, I-types and some A-types.|||||Slightly-moderately porphyritic basaltic andesite, andesite and basalt; also crystal-rich rhyolitic ignimbrite, rhyolite to dacite lava, and tuffaceous rocks; subordinate sediments.|
68736|Mount Lookerbie gravels|60282|6|Mentioned|p52|||Informal reference to gravelly units in the region of Mount Lookerbie.||||||
36500|Mount Low complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 142.  I-Type.||||||
80777|Mount Mackenzie Granite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Buff to pale brown, medium-grained, slightly porphyritic, leucocratic muscovite-biotite monzogranite; granophyric; commonly deformed and partly recrystallise.|
30707|Mount Maggie Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite (part of the Wonga Batholith). Intrudes the Argylla Formation. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30707|Mount Maggie Granite|50536|5|Briefly described|p1.4, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.||||||07-NOV-08
30707|Mount Maggie Granite|73137|4|Described|p2, p5, p7, p9-13, p16|Statherian|Statherian|Wonga Igneous Subprovince. Geochron is magmatic crystallisation age; matches younger end of previous Wonga Igneous Subprovince ages. Sample is from the eastern margin of a prominent structural dome in the central Mary Kathleen Domain (different composition but very similar to the age of the quartz diorite from the interior of the dome). Sample also yielded a metamorphic age of 1526 +/- 16 Ma. [See article for Mount Maggie Granite sample field description, petrographic description and detailed geochronology].|1729 +/- 6 Ma|||Intrudes Corella Formation, Ballara Quartzite.|Includes coarsely porphyritic and strongly foliated biotite granite/syenogranite.|11-OCT-22
30707|Mount Maggie Granite|73553|4|Described|p65, p73, p74 Tb 4.1.2, p83, p89-p99|Statherian|Statherian|Mary Kathleen Domain. Wonga Igneous Subprovince. Formerly mapped as Wonga Granite, as subunit '2' in the west and far north, and subunit '1' in the north. Outcrops sporadically in a belt 35 km from north to south and ~9 km east to west. Distribution shown is similar to Bastrakova et al., (2001) with boundaries from more detailed surface geology (GSQ, 2018). Low subdued magnetic response. Significant differences in radiometric response across unit. Age from Kositcin et al., (2019), Kositcin et al., (2021). In contact with Corella Formation in current mapping, but may be Argylla Formation or Ballara Quartzite based on geochronology. Common aplitic and pegmatite veins.|~1730 Ma U-Pb SHRIMP|||Faulted contact with Natalie Granite to the south, interpreted to intrude Argylla Formation|Strongly foliated, porphyritic, biotite +/- amphibole monzogranite to syenogranite with allanite and fluorite as accessory phases; local granodiorite and fine-grained equigranular biotite-amphibole monzogranite; local mingling with a mafic phase.|03-FEB-23
75734|Mount Magnus Granite|70740|5|Briefly described|p34, p127|||Outcrop characteristics and distribution briefly discussed. Appears to also intrude Peak John Well Granite units. ||||Intrudes the Ukalunda Formation.|Leucocratic, porphyritic biotite monzogranite, light pink to orange, medium-grained, porphyritic biotite granodiorite.|
30718|Mount Margaret Granite|23519|5|Briefly described|p128|Mesoproterozoic|Mesoproterozoic|See also page 111 Table 1. Age: 1530+/-8 Ma (U-Pb).||||||
30718|Mount Margaret Granite|23967|5|Briefly described|p1331 Table 1|Mesoproterozoic|Mesoproterozoic|Mount in Mt in text.||||||
30718|Mount Margaret Granite|24197|5|Briefly described|p96 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Age: 1530Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30718|Mount Margaret Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Mount is Mt. in text. Geological Province: Mount Isa Block. Age: ~1544-1521Ma (U-Pb).||||||
30718|Mount Margaret Granite|24257|5|Briefly described|p72 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological Province: Eastern fold belt, Mount Isa Block.||||||
30718|Mount Margaret Granite|24259|6|Mentioned|p104|||Geological Province: Mount Isa Block.||||||
30718|Mount Margaret Granite|43490|6|Mentioned|8||Phanerozoic|||||||
30718|Mount Margaret Granite|50100|6|Mentioned|p13 Fig.4|Calymmian|Calymmian|Mount is Mt in text.||||||
30718|Mount Margaret Granite|50332|5|Briefly described|p22, p62|Mesoproterozoic|Mesoproterozoic|Of the Williams and Naraku Batholiths. Age: ~1545-1530Ma. Geological Province: Quamby-Malbon and Cloncurry Subprovinces.||||||13-MAY-14
30718|Mount Margaret Granite|50536|5|Briefly described|p1.5, 11.4, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Mount Margaret Suite. Age: 1530-1528 +/- 8Ma.||||||
30718|Mount Margaret Granite|60665|6|Mentioned|p1157 Fig.9. |Calymmian|Calymmian|Northern Cloncurry intrusion. Age inferred from Fig.9.|1530 +/- 8 Ma.|||||
30718|Mount Margaret Granite|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Age: 1530-1520 Ma.||||||
30718|Mount Margaret Granite|61936|5|Briefly described|p200|Mesoproterozoic|Mesoproterozoic|Y-undepleted sodic intrusion.  Age: ca1530Ma. Mount is Mt in text. ||||||
30718|Mount Margaret Granite|61963|5|Briefly described|p791|Mesoproterozoic|Mesoproterozoic|Age: ca.1530Ma (Page and Sun 1998).||||||
30718|Mount Margaret Granite|64250|6|Mentioned|p11 fig 3|||Cloncurry Fold Belt, Mount Isa Inlier.|1530 +/-8 Ma; 1528 +/- 6 Ma.|||||
30718|Mount Margaret Granite|65396|5|Briefly described|p7, p53, p55-56, p82, p84, p89, p97-98|Calymmian|Calymmian|See also p157, p175, p241, p388, p440. Cloncurry Fold Belt. Eastern succession. Appears as Mount Margaret granite on p53. Whole-rock geochemistry detailed.|1530 +/- 8 Ma, 1528 +/- 6 Ma (SHRIMP)||||A-type. Composed largely of K-poor, sodic granitic intrusions.|04-APR-17
30718|Mount Margaret Granite|66913|5|Briefly described|p170 fig 1, p171 fig 2, p187|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2. Possibly hydrothermal zircons dated at 1528+/-6 Ma.|Magmatic age 1530+/-8 Ma.|||||
30718|Mount Margaret Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p17|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Canobie Domain, Mount Isa Inlier. Forms isolated outcrops surrounded by cover rocks east of Ernest Henry. Williams Igneous Event.|1530 +/- 8 Ma (Page and Sun, 1998).|Williams Supersuite.|||Granite, albitised granite|
30718|Mount Margaret Granite|68542|6|Mentioned|p16 fig 4|||An intrusive phase of the Williams/Naraku Batholith.||||||
30718|Mount Margaret Granite|68576|6|Mentioned|Q_2: p16|||An intrusive phase of the Williams/Naraku Batholith.||||||
30718|Mount Margaret Granite|69056|5|Briefly described|p56, Time-Space plot sheet|Calymmian|Calymmian|Constantine Domain.|1530 +/- 8 Ma (Page and Sun, 1998).|Williams Supersuite.|||Granite and albitised granite.|
30718|Mount Margaret Granite|69591|5|Briefly described|p59||||1530 +/- 8 Ma (Page and Sun, 1998).|Williams Supersuite.|||Granite, albitised granite.|
30718|Mount Margaret Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1530+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)|||||
30718|Mount Margaret Granite|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1530 +/- 8 Ma|||||
30718|Mount Margaret Granite|72949|6|Mentioned|p35|Calymmian|Calymmian|Mount Isa Inlier, Western Fold Belt.||||||
30718|Mount Margaret Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1528 +/- 6 Ma|||||
78941|Mount Maryvale Granodiorite|65388|2|Defined|p375, p135 Fig. 53, p362, 364, 365, 383|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. May be intruded by Strathdee Granodiorite. Probable age given. Contact with Mount Spencer Granodiorite may be faulted. Pale brownish grey, buff, or brown to dark reddish brown, medium to fine-grained, uneven-grained to porphyritic granodiorite.||||||
36180|Mount Masterson Granodiorite|23506|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Almaden Supersuite.||||||
36180|Mount Masterson Granodiorite|60425|4|Described|p282-3 Appdx.|Early Permian|Late Carboniferous|Uanssigned. I-type. Grey, fine- to medium-grained hornblende granodiorite.||||||07-FEB-11
36309|Mount Max Granite|23291|4|Described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Newcastle Range A-types. Geological Province: Georgetown Region.||||||08-JUL-15
36309|Mount Max Granite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Cumbana Batholith, O'Briens Supersuite.||||||
82984|Mount McMaster Basalt|73115|6|Mentioned|p28, p39, p43, p48, p53, p59, p65|Pliocene|Pliocene|[See also 'Mount McMasters' Basalt p29]. McBride Basalt Province.|2.7 Ma|||||
23825|Mount Mia Serpentinite|22845|2|Defined|p4,12-14,28-34,|Early Carboniferous|Late Devonian|Intruded by the Station Creek Granodiorite||||||24-NOV-05
23825|Mount Mia Serpentinite|22846|6|Mentioned|p14,37,8,58,68|Carboniferous|Devonian|Intruded by trhe Station Creek Quartz Monzonite.||||||
23825|Mount Mia Serpentinite|23251|5|Briefly described|Table 1 p16, p5|||North D'Aguilar Subprovince, Wandilla Province. Max thickness ~4 km.||||||30-NOV-05
23825|Mount Mia Serpentinite|23608|6|Mentioned|p54|||||||||
23825|Mount Mia Serpentinite|42694|5|Briefly described|map legend|Carboniferous|Pre-Carboniferous|||||||
23825|Mount Mia Serpentinite|43092|4|Described|p14|||see also map enclosure||||||
23825|Mount Mia Serpentinite|43588|6|Mentioned|p30||Late Devonian|||||||
23825|Mount Mia Serpentinite|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
23825|Mount Mia Serpentinite|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
23825|Mount Mia Serpentinite|44928|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
23825|Mount Mia Serpentinite|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
23825|Mount Mia Serpentinite|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince. Serpentinite and serpentinite matrix melange with blocks of serpentinite, mafic greenschist and locally phyllite.||||||
23825|Mount Mia Serpentinite|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|North D'Aguilar Subprovince.||||||
23825|Mount Mia Serpentinite|68679|5|Briefly described|p320-321, p326, p328-332, p387, p470|||Little et al. (1992); Litle et al. (1993). Includes areas previously mapped as Mary Valley Serpentinite (Wilkinson, 1951) and unnamed serpentinite in the Kilkivan area (Murphy et al., 1976). Forms two NNW-trending belts in the central part of the North D'Aguilar Subprovince, and several smaller bodies near Kilkivan. Forms steep rugged hills and plateaus covered by a unique grasstree flora. ~200-4000m thick. A lower plate melange, exposed by late Carboniferous extension. Unusual lithology described in some detail. RELATED UNITS (continued): Is faulted under Anderson Creek Phyllite, Kandanga Creek Megabreccia and Amamoor beds. Is intruded by Rush Creek Granodiorite. Encloses blocks of Widgee Metamorphics and Talamy Schist. Is correlated with Pine Mountain Serpentinite and (parts of) Rocksberg Greenstone.||||Structurally overlies Widgee, Wongella and Gobongo Metamorphics (and is faulted against the last). Is overlain unconformably by Neara Volcanics and North Arm Volcanic Group. See COMMENTS for more.|Metamorphosed serpentinite-matrix melange, reworked serpentinitic sediment; lenses of biotite-muscovite schist, greenschist blocks, rounded marble clasts and crossite-albite schist.|
69842|Mount Misery Granite (QLD)|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||01-DEC-05
69842|Mount Misery Granite (QLD)|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Muscovite-biotite granite.||||||01-DEC-05
69842|Mount Misery Granite (QLD)|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Grey, muscovite-biotite granite; locally strongly deformed.|
69842|Mount Misery Granite (QLD)|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Grey, muscovite-biotite granite; locally strongly deformed.|
29614|Mount Mitchell Suite|43005|5|Briefly described|p216|||Related to Mount Mitchell nepheline benmoreite?||||||
29614|Mount Mitchell Suite|71628|5|Briefly described|p11: 17, 21|||||Bungulla Supersuite.|Mount Mitchell Monzogranite.|||
34036|Mount Morgan Trondhjemite|22482|4|Described|p487, Fig.1||Middle Devonian|Age of 377+/-5 Ma||||||
34036|Mount Morgan Trondhjemite|23468|6|Mentioned|p 309|||||||||
34036|Mount Morgan Trondhjemite|24399|5|Briefly described|p271, p277|Middle Devonian|Middle Devonian|Calc-alkaline I-type granitoid rocks (Roberts and Clemens, 1993).  Mount is Mt. in text.  Geological Province: New England Fold Belt.||||||
34036|Mount Morgan Trondhjemite|24521|5|Briefly described|p101, p108 Fig. 2|Devonian|Devonian|Relatively small intrusion 20km long and 4km wide. Geological Province: northern New England Orogen.||||||04-MAY-05
34036|Mount Morgan Trondhjemite|24615|5|Briefly described|CD|Middle Devonian|Middle Devonian|[Dgmo/d].  Grey medium-grained hornblende diorite, quartz diorite, gabbro.||||||
34036|Mount Morgan Trondhjemite|50317|5|Briefly described|Map Legend|Devonian|Devonian|||||||28-MAY-04
34036|Mount Morgan Trondhjemite|61147|5|Briefly described|pp375-378.  |Middle Devonian|Middle Devonian|Formerly referred to as a tonalite. Also shown as Mount Morgan trondhjemite.|377 +/- 5 Ma (Golding in Hayward et al. 1999).|||Intrudes Capella Creek Group. Is overlain unconformably by the Mount Hoopbound Formation.||
34036|Mount Morgan Trondhjemite|61730|5|Briefly described|p1000 Fig.3|Late Devonian|Late Devonian|Intrudes the Mount Warner Volcanics from which it is geochemically indistinguishable. Geological Province: Yarrol Province. See also p1001.||||||
34036|Mount Morgan Trondhjemite|63600|5|Briefly described|p917|Middle Devonian|Middle Devonian|Age: 380Ma. (U-Pb zircon). Mount is mt in text.||||||07-FEB-11
34036|Mount Morgan Trondhjemite|68008|3|Fully described|p26, p29-33, p39-40, p51-52, p55, p61-62|Middle Devonian|Middle Devonian|See also p67, p294-295, p307-318, p320, p477, p480, p483, p487-488, p527, p568, p578-579. Previously Mount Morgan Tonalite (Kirkegaard et al., 1970). Name is changed in this study to reflect the dominant lithology. Forms a SE-trending belt 25 x 4 km. Crops out as boulder-sized rubble. Massive and apparently undeformed. Encloses a roof pendant of Mine Corridor Volcanics (now Mount Warner Volcanics), which hosts the Mount Morgan Au-Cu deposit. Geochemistry discussed in detail: similar to Capella Creek Group. Several other age determinations given.|379.9 +/- 4.27 Ma (U-Pb zircon).|||Intrudes Raspberry Creek Formation, Mount Warner Volcanics, Capella Creek Group. Is overlain nonconformably by Mount Hoopbound Formation.|Trondhjemite, lesser tonalite, quartz diorite to quartz gabbro; medium-grained, locally porphyritic; quartz-rich, K-minerals poor; breccia pipes. Ubiquitous micrographic quartz-plagioclase intergrowths. Lithologies described, illustrated in detail.|
34036|Mount Morgan Trondhjemite|68553|6|Mentioned|Map legend; schematic diagram.|Late Devonian|Middle Devonian|Calliope Province. This unit, as well as the Pomegranate Tonalite and unnamed Middle-Late Devonian plutonic units, are all mapped under the same symbol, Dgm.||||||
34036|Mount Morgan Trondhjemite|68679|5|Briefly described|p312, p315, p338-339, p399,p401-403,p424|Late Devonian|Middle Devonian|Rockhampton Subprovince, northern New England Orogen. Previously the Mount Morgan Tonalite. Extensive unit: ~25km long and 3-4km wide. Is geochemically indistinguishable from the Mount Warner Volcanics, but is ~15 m.y. younger. K-Ar and Ar-Ar age determinations range widely, most in the range 377-364 Ma.|379.9 +/- 4.27 Ma (SHRIMP U-Pb: Fanning, 2012).|||Is overlain by Mount Hoopbound Formation. Surrounds the Mine Corridor Volcanics (Mount Warner Volcanics roof pendant). Intrudes Capella Creek Group.|Mostly trondhjemite; also tonalite, quartz diorite, quartz gabbro, breccia. Local porphyritic texture and breccia pipes imply high-level emplacement.|
34036|Mount Morgan Trondhjemite|71592|5|Briefly described|Appendix A.|||New England Orogen.|380+/-4.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
34036|Mount Morgan Trondhjemite|73179|6|Mentioned|p1152|Frasnian|Givetian|New England Orogen, northern. Geochron from Murray et al. (2012).|379.9 +/- 4.27 Ma|||||
36785|Mount Mucki Diorite|23608|3|Fully described|p54||Triassic|Replaces Mount Mucki Complex.  Also see page 50 fig.1 and page 49 fig.2. K/Ar 210Ma. I-Type granite. Intrudes Neara Volcanics, Highbury Volcanics, Woonga Granodiorite and Woolooga Granodiorite. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36785|Mount Mucki Diorite|50320|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
36785|Mount Mucki Diorite|68679|6|Mentioned|p411|||Tang and Gust (2000). Subsequently the Mount Mucki Complex.||||||
26767|Mount Mulligan Coal Measures|12575|5|Briefly described|p781, p784 Table 1.|||Apatite fission track analyses, vitrinite reflectance data are detailed. A new vitrinite reflectance value of 0.73% shows the Permian units have experienced high palaeotemperatures at some time since deposition[ probably in the Cretaceous].|270-245 Ma.|||||07-SEP-18
26767|Mount Mulligan Coal Measures|23422|5|Briefly described|Plate 7.3|Permian|Early Carboniferous|||||||
26767|Mount Mulligan Coal Measures|23423|4|Described|Table 7.2 p300|Late Permian|Permian|Also see p258 + p298. Underlying unit Hodgkinson Formation - unconformable. Maximum thickness ~450 m.||||||
26767|Mount Mulligan Coal Measures|23430|4|Described|p516|||Underlying Unit Hodgkinson Formation and Featherbed Volcanic Gp - unconformably. Ngarrabullan Basin Province.||||||
26767|Mount Mulligan Coal Measures|23431|5|Briefly described|p539|||||||||
26767|Mount Mulligan Coal Measures|24086|5|Briefly described|p312 Fig. 1|Late Permian|Late Permian|||||||
26767|Mount Mulligan Coal Measures|30914|6|Mentioned|Map legend|Permian|Permian|||||||
26767|Mount Mulligan Coal Measures|31832|6|Mentioned|Table 6|||||||||
26767|Mount Mulligan Coal Measures|32835|6|Mentioned|p6|||Flora||||||
26767|Mount Mulligan Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
26767|Mount Mulligan Coal Measures|37065|5|Briefly described|p32|||||||||
26767|Mount Mulligan Coal Measures|37095|6|Mentioned|p246|||||||||
26767|Mount Mulligan Coal Measures|37098|4|Described|p253|||||||||
26767|Mount Mulligan Coal Measures|37575|4|Described|p179|||||||||
26767|Mount Mulligan Coal Measures|37613|6|Mentioned|p247|||See also Fig.7.||||||
26767|Mount Mulligan Coal Measures|39252|6|Mentioned|Fig. 15|||||||||
26767|Mount Mulligan Coal Measures|39261|6|Mentioned|Fig. 9|||||||||
26767|Mount Mulligan Coal Measures|39264|6|Mentioned|p156|||||||||
26767|Mount Mulligan Coal Measures|39266|6|Mentioned|p222|||||||||
26767|Mount Mulligan Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9||||||
26767|Mount Mulligan Coal Measures|42681|4|Described|p22|||||||||
26767|Mount Mulligan Coal Measures|43013|6|Mentioned|p242|||actually spelt Mt Mulligan Coal Measures||||||
26767|Mount Mulligan Coal Measures|43151|5|Briefly described|Map legend|Late Permian|Late Permian|||||||
26767|Mount Mulligan Coal Measures|43285|5|Briefly described|Map Legend||Late Permian|||||||
26767|Mount Mulligan Coal Measures|43625|3|Fully described|p38,44|Late Permian|Permian|(Middle Permian)||||||12-JAN-05
26767|Mount Mulligan Coal Measures|43626|6|Mentioned|p15|Triassic|Late Permian|||||||
26767|Mount Mulligan Coal Measures|43665|6|Mentioned|p21||Permian|||||||
26767|Mount Mulligan Coal Measures|43896|14|Not recorded|Map Legend||Late Permian|||||||
26767|Mount Mulligan Coal Measures|43898|14|Not recorded|Map Legend||Late Permian|||||||
26767|Mount Mulligan Coal Measures|43984|14|Not recorded|p134|||||||||
26767|Mount Mulligan Coal Measures|44053|14|Not recorded|p239|||||||||
26767|Mount Mulligan Coal Measures|44425|14|Not recorded|p14,15,19,22,31,|||opp.11, map. See also Lexicon. Fossils.||||||26-APR-13
26767|Mount Mulligan Coal Measures|44913|14|Not recorded|p57,Fig.3,63|||||||||
26767|Mount Mulligan Coal Measures|45025|2|Defined|p61-2||Late Permian|||||||
26767|Mount Mulligan Coal Measures|46845|6|Mentioned|Table 1|||||||||
26767|Mount Mulligan Coal Measures|50316|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Ngarrabullgan Basin.||||||
26767|Mount Mulligan Coal Measures|60425|3|Fully described|p5, p14 Tb. 1, p37-38|Late Permian|Middle Permian|Unconformable on Hodgkinson Fm; overlain disconcordantly by Pepper Pot Sst; also angular discordance on Breccia Creek Rhyolite. Max. thickness: ~450m. Detailed lithology included for the four irregularly distributed subunits (unnamed) of the formation.||||||07-FEB-11
26767|Mount Mulligan Coal Measures|62371|5|Briefly described|p472 Fig.3|Permian|Permian|Deep marine sediments.||||||
26767|Mount Mulligan Coal Measures|62523|4|Described|p13|Late Permian|Late Permian|Divided into 4 unnamed subunits of variable lithologies and thicknesses ranging from 10m to 80m. Overlies Breccia Creek Rhyolite; overlain by Pepper Pot Sandstone.See also map and legend at p3-4.||||||07-FEB-11
26767|Mount Mulligan Coal Measures|63140|6|Mentioned|p572 fig 3|Permian|Permian|Hodgkinson Province.||||||
26767|Mount Mulligan Coal Measures|63154|5|Briefly described|p281 Fig. 3|Permian|Permian|Geological province: Hodgkinson Province.||||||11-APR-07
26767|Mount Mulligan Coal Measures|64665|5|Briefly described|p53 Fig.2.|Late Permian|Late Permian|Ngarrabullan Basin. Named after a prominent mesa which dominates the area. Up to 149 m thick. Resources remain poorly constrained: estimated resources range from 45 - 90 Mt. Seams vary in thickness from 0.4 to 1.7 m. High volatile bituminous rank.||||Is overlain by Pepper Pot Sandstone.||
26767|Mount Mulligan Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Ngarrabullgan Basin.||||||
26767|Mount Mulligan Coal Measures|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|269 +/- 8 Ma (SHRIMP).|||||
26767|Mount Mulligan Coal Measures|69592|5|Briefly described|p243-244|Permian|Permian|Ngarrabullgan Basin. Up to ~450m thick; thins and wedges out to the S. Fluviatile, lacustrine and mire deposits. Contains late Permian paylnomorphs and plant macrofossils.||||Unconformably overlies Hodgkinson Formation and Featherbed Volcanic Group. Is overlain by Pepper Pot Sandstone.|Medium- to very thick-bedded, massive, pebbly volcaniclastic sandstone and fine breccia; then thin-bedded carbonaceous siltstone and claystone, with interbeds of fine-grained sandstone and coal seams; then interdigitating conglomerate and sandstone.|
26767|Mount Mulligan Coal Measures|70207|6|Mentioned|p74|Permian|Permian|||||||
26767|Mount Mulligan Coal Measures|70345|6|Mentioned|p3|Permian|Permian|||||||
26767|Mount Mulligan Coal Measures|70673|6|Mentioned|p7|Permian|Permian|||||||
26767|Mount Mulligan Coal Measures|72297|5|Briefly described|p697|Permian|Permian|Ngarrabullgan Basin. Coal was extracted from three thin separate seams by underground mining during 1910-1957.||||||
26767|Mount Mulligan Coal Measures|72983|6|Mentioned|p15|Permian|Permian|||||||
23827|Mount Newsome Granodiorite|42614|6|Mentioned|Table 2 P10|||Reserved, Crouch & Withnall 1991.||||||
23827|Mount Newsome Granodiorite|42747|5|Briefly described|p37, Fig.9|||||||||
23827|Mount Newsome Granodiorite|43029|2|Defined|p22||Middle Devonian|Rb-Sr dating of 372-382 Ma. See also Fig.2,p16||||||
23827|Mount Newsome Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
23827|Mount Newsome Granodiorite|43213|3|Fully described|p33, p56, p95-98, p104-105, p109-110|Devonian|Devonian|See also p116-121, p174-175, p178, p208, p210-211, p220-222, p233, p241, p243. Type locality and geophysical properties described. Extensive component of the Retreat Batholith. Has local foliation from Middle Devonian deformation. Rb-Sr dating of several biotite-whole rock pairs gave an age range of 372-382 Ma +/- 3 Ma (Carr, pers. comm., 1993). Geochemistry, modal and chemical analyses and geophysics detailed.|370 Ma (K-Ar biotite: Webb and McDougall, 1968).|||Intrudes Bathampton Metamorphics, Anakie Metamorphic Group, Gem Park Granite and Whitdale Granodiorite. Is intruded by Hoy Basalt. Is overlain unconformably by Silver Hills Volcanics.|Dominantly grey, fine- to coarse-grained, equigranular to porphyritic biotite-hornblende granodiorite.|
23827|Mount Newsome Granodiorite|43861|5|Briefly described|28||Devonian|Intrudes Bathampton Metamorphics||||||
23827|Mount Newsome Granodiorite|68482|5|Briefly described|Map Legend|Tournaisian|Frasnian||375 +/- 3 Ma, Rb-Sr (biotite). ||||Grey, fine to coarse-grained, equigranular to porphyritic biotite-hornblende granodiorite; subordinate light grey, fine-grained biotite granite.|
23827|Mount Newsome Granodiorite|68731|5|Briefly described|p132, p133, p134, p135, p135 Fig 3F3.3|Upper Devonian|Lower Devonian||392.4 +/- 10.2 Ma, U-Pb (SMRIMP)|Of the Mount Newsome Suite.||Intrudes the Gem Park Granite, Bathampton Metamorphics, and Whitdale Granodiorite.||
23827|Mount Newsome Granodiorite|69952|5|Briefly described|p123|Middle Devonian|Middle Devonian|Part of the Retreat Batholith in the southern Anakie Province.|392.4 +/- 10.2 Ma (SHRIMP; Wood and Lister, 2013).|||||30-NOV-15
23827|Mount Newsome Granodiorite|70499|5|Briefly described|p5|||Mean U-Pb SHRIMP age of 392 Ma (Middle Devonian; Wood, 2006). Also contains biotite with recalculated K-Ar age of 370 Ma (Webb and McDougall, 1968; Withnall et al., 1995).||||Intruded into Anakie Metamorphic Group.||
23827|Mount Newsome Granodiorite|70856|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey, fine- to coarse-grained, equigranular to porphyritic biotite-hornblende granodiorite; subordinate light grey, fine-grained biotite granite.|
23827|Mount Newsome Granodiorite|71966|5|Briefly described|p1001|Eifelian|Eifelian|Geological province: Anakie Province, Thomson Orogen. Of the Retreat Batholith. Outcropping equivalent to felsic rhyolitic ignimbrite undercover in the Thomson Orogen; together represents evidence for a Devonian felsic volcanic province.|392.4+\-10.2 Ma (Wood and Lister 2013)|||||
23827|Mount Newsome Granodiorite|73179|6|Mentioned|p1152|Frasnian|Emsian|Anakie Inlier. Retreat Batholith. Geochron from Wood and Lister (2013).|392.4 +/- 10.2 Ma|||||20-SEP-22
77639|Mount Newsome Suite|43213|6|Mentioned|p117|||||Unit in Retreat Supersuite.|Includes Mount Newsome and Whitdale Granodiorites.|||
77639|Mount Newsome Suite|68731|6|Mentioned|p132||||||Includes the Mount Newsome Granodiorite.|||
30594|Mount Noble Granite|50198|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||||||
30594|Mount Noble Granite|68354|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Age min: Early Permian?|||||Pink to white, coarse-grained equigranular biotite granite.|03-JUL-15
75668|Mount Nutt Granite|68679|5|Briefly described|p362, p366 Fig.5.57|Mississippian|Mississippian|Northern Connnors Subprovince. Unfoliated. REE plot.|341.3 +/- 2.4 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75668|Mount Nutt Granite|68901|5|Briefly described|p4, p47-49, p145|Carboniferous|Carboniferous|Northern New England Orogen, Bowen Region. Underlies most of the township of Bowen. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|341.3 +/- 2.4 Ma (SHRIMP U-Pb)||||Pale-grey, medium-grained, uneven grained to slightly porphyritic, leucocratic biotite monzogranite with traces of titanite.|28-SEP-18
75668|Mount Nutt Granite|70673|6|Mentioned|p9|Carboniferous|Carboniferous|||||||
23828|Mount Observatory Granite|42747|5|Briefly described|p37|||||||||
23828|Mount Observatory Granite|43029|2|Defined|p19||Middle Devonian|K-Ar date of 373 Ma. See also Fig.2,p16||||||
23828|Mount Observatory Granite|43213|3|Fully described|p95-97, p104-107, p116-121, p174-175|Devonian|Devonian|See also p178-179, p208, p222, p232, p240, p242. Type locality is Mount Observatory. High K, U and Th radiometric responses. Component of the Retreat Batholith. Many small plugs of Hoy Basalt were intruded along the fault boundary between this unit and Kilmarnock Granodiorite. Peraluminous. Geochemistry, modal and chemical analyses and geophysics detailed. Appears as Mount Observatory Granodiorite on p174.|373 Ma (K-Ar biotite: Webb and McDougall, 1968).|||Intrudes Monteagle Quartzite. Partly faulted against Kilmarnock Granodiorite.|Grey to light grey, fine- to medium-grained biotite granite; common metasedimentary xenoliths to 1m and sparse quartz eyes; biotite clots or glomercrystic intergrowths to 4mm are characteristic.|
23828|Mount Observatory Granite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||373 +/- 7 Ma, K-Ar (biotite).||||Grey, fine to medium-grained, equigranular biotite granite.|01-SEP-14
25735|Mount Oxide Chert Member|23031|5|Briefly described|26|||Geol province Lawn Hill Subprovince. Parent McNamara Group||||||
25735|Mount Oxide Chert Member|23073|5|Briefly described|p744 (fig 2)|||||||||
25735|Mount Oxide Chert Member|23393|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of Paradise Creek Formation.||||||07-NOV-08
25735|Mount Oxide Chert Member|24419|6|Mentioned|p18|||Of the Paradise Creek Formation.||||||
25735|Mount Oxide Chert Member|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|Reserved as Oxide Chert Member.||||||
25735|Mount Oxide Chert Member|37459|1|Redefined|p429|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
25735|Mount Oxide Chert Member|38237|4|Described|p128|||||||||
25735|Mount Oxide Chert Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25735|Mount Oxide Chert Member|38310|6|Mentioned|p237|||||||||
25735|Mount Oxide Chert Member|38348|6|Mentioned|p9|||||||||
25735|Mount Oxide Chert Member|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of Paradise Creek Formation (basal). Grey laminated chert.||||||15-JUN-06
25735|Mount Oxide Chert Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25735|Mount Oxide Chert Member|39944|6|Mentioned|Fig.5|||||||||
25735|Mount Oxide Chert Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25735|Mount Oxide Chert Member|40221|5|Briefly described|p16|||||||||
25735|Mount Oxide Chert Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
25735|Mount Oxide Chert Member|43235|5|Briefly described|p9,Fig.10.|||of Paradise Creek Formation.||||||
25735|Mount Oxide Chert Member|45166|5|Briefly described|p30|||||||||
25735|Mount Oxide Chert Member|47083|5|Briefly described|p16|||Basal unit in Paradise Creek Formation. Of Paradise Creek Formation. Maximum thickness: 10 m.||||||
25735|Mount Oxide Chert Member|50332|6|Mentioned|p21|Proterozoic|Proterozoic|Of the Paradise Creek Formation.||||||07-FEB-11
25735|Mount Oxide Chert Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.||McNamara Group|||Grey laminated chert.|
36183|Mount Peter Granite|23497|5|Briefly described|Table 1||Early Permian|of Kennedy Province. Intrudes Hodgkinson Formation rocks. Lithologically similar to Tinaroo Granite.||||||
36183|Mount Peter Granite|23507|5|Briefly described|Map Legend||Early Permian|||||||
36183|Mount Peter Granite|60425|4|Described|p56 Tb. 4|Early Permian|Early Permian|Of the Bellenden Ker Supersuite. Age: 280+/-4ma (SHRIMP). One of several units of this supersuite to intrude the Hodgkinson Formation. Detailed lithology of these porphyritic granites is incuded. S-type.||||||07-FEB-11
23829|Mount Pike Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|284-255 Ma.|Unit in Whypalla Supersuite.||||
23829|Mount Pike Granite|23423|5|Briefly described|p248|||Of Whypalla Supersuite.||||||01-JUN-09
23829|Mount Pike Granite|23511|5|Briefly described|Map Legend||Early Permian|Age: 284 +/- 4Ma.||||||
23829|Mount Pike Granite|24086|6|Mentioned|p312 Fig. 1|||Mount is Mt. in text.||||||
23829|Mount Pike Granite|24213|5|Briefly described|p777|Permian|Permian|Mount is Mt. in text.||||||
23829|Mount Pike Granite|42304|2|Defined|p28|Permian|Carboniferous|Not dated, age assumed. Reserved April 1988 by R.J. Bultitude.||||||
23829|Mount Pike Granite|43098|1|Redefined|p31|Early Permian||U-Pb age of 284+/-4 Ma.||||||
23829|Mount Pike Granite|43111|6|Mentioned|p38|||Of Whypalla Supersuite.||||||01-JUN-09
23829|Mount Pike Granite|43625|5|Briefly described|p123, Appendix 6|||||||||
23829|Mount Pike Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
23829|Mount Pike Granite|50596|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Whypalla Supersuite.  Biotite adamellite.||||||
23829|Mount Pike Granite|50630|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 284 +/- 4Ma (SHRIMP).  Of the Whypalla Supersuite.||||||14-JUN-13
23829|Mount Pike Granite|60425|4|Described|p276-7 Appdx.|Early Permian|Early Permian|Of Mount Pike Suite (Whypalla Supersuite). S-type. Age: 284+/-4Ma (SHRIMP). White to pale grey, fine- to coarse-g.,slightly-highly porphyritic musc.-biotite-granite; accessory garnet, zircon, apatite, ilmenite, monazite?, rutile; enclaves to~40cm common||||||07-FEB-11
23829|Mount Pike Granite|69593|5|Briefly described|p479, p481 Fig.6.4(a), p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|284 +/- 4 Ma.|Mount Pike Suite.|||S-type.|
30144|Mount Pike Suite|43098|6|Mentioned|p31|||of Whypalla Supersuite||||||
30144|Mount Pike Suite|60425|5|Briefly described|p81 Tb. 5|Early Permian|Early Permian|Of the Whypalla Supersuite. Contains Mount Pike and Bullhead Granites. Age of crystallisation: 284+/-4Ma.||||||07-FEB-11
30144|Mount Pike Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Mount Pike, Bullhead Granites.|||
27648|Mount Podge Limestone|23422|5|Briefly described|p180, p206 Table 6.3|Middle Devonian|Early Devonian|Of  Wilkie Gray Group.  Previously included in the Fanning River Group.||||||
27648|Mount Podge Limestone|23430|5|Briefly described|p505|||Of Wilkie Gray Group||||||
27648|Mount Podge Limestone|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|of Wilkie Gray Group.||||||
27648|Mount Podge Limestone|23522|5|Briefly described|p250 Fig 6||Emsian|Mount is Mt. in text. Of Wilkie Gray Group.||||||
27648|Mount Podge Limestone|23893|5|Briefly described|p15|Eifelian|Emsian|Of Wilkie Gray Group. Geological Province: Camel Creek Subprovince.||||||04-FEB-08
27648|Mount Podge Limestone|24577|4|Described|p752 Fig. 1|Emsian|Pragian|Of the Wilkie Gray Group. Unconformably overlies the Argentine and Running River Metamorphics. Limestone is Ls in text. Geological Province: Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
27648|Mount Podge Limestone|24610|5|Briefly described|p64|Givetian|Emsian|Geological Province: Burdekin Basin. Of Zhen (1991).||||||
27648|Mount Podge Limestone|24611|5|Briefly described|p193|Emsian|Emsian|Dominantly packstones and calcirudites. Thickness in type section: 156m. Overlain by Keelbottom Group. Geological Province: Burdekin Basin.  See also p194 Fig. 1 and p196 Fig. 2.||||||04-FEB-08
27648|Mount Podge Limestone|24612|4|Described|p8|Devonian|Devonian|Of Fanning River Group. Overlies Laroona Formation (conformable in Mount Podge area). Max. thickness: 300 m. Previously of Burdekin Formation - now proposed to be of Fanning River Group in the Mount Podge area.||||||
27648|Mount Podge Limestone|24613|2|Defined|p9 Fig. 4, p13-14, Tb. 1|Eifelian|Emsian|Of Fanning Group. Contains the Carlinastrea limestone lens. Conformable/gradational on Laroona Fm; unconformable below Myrtlevale Fm. Max.thickness: 304.5m. Geol.prov: Burdekin Basin. Fossiliferous l'st. (corals, stromatoporoids), minor siltst.+ sst.||||||07-FEB-11
27648|Mount Podge Limestone|24614|5|Briefly described|p191 Fig. 1|||Of Wilkie Gp; formerly of Fanning River Gp. Shallow marine limestones of diverse lithologies, with basal sequence transitional from the underlying Laroona Arkose. Overlain by Burdekin Lst. Geol Prov: Burdekin Basin. See also p193 Fig. 2.||||||07-FEB-11
27648|Mount Podge Limestone|42689|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
27648|Mount Podge Limestone|42690|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
27648|Mount Podge Limestone|42933|5|Briefly described|Fig.94 p258|||Actually listed as just Mt Podge.||||||
27648|Mount Podge Limestone|43095|5|Briefly described|Plate 2|||of Fanning River Group.||||||
27648|Mount Podge Limestone|65214|6|Mentioned|p275, p278|Devonian|Devonian|QLD, Mount Podge. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27648|Mount Podge Limestone|65940|6|Mentioned|p203-204|Emsian|Emsian|Contains A. clermontense (see Zhen, 1995); Phillipsastrea maculosa (serotinus Zone; Zhen, 1995).||||||
27648|Mount Podge Limestone|68350|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.||Unit in Wilkie Gray Group.||Conformably overlies Laroona Formation.|Fossiliferous limestone (calcirudite, calcarenite and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone.|
27648|Mount Podge Limestone|68351|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.||Unit in Wilkie Gray Group.||Conformably overlies Laroona Formation.|Fossiliferous limestone (calcirudite, calcarenite and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone.|
27648|Mount Podge Limestone|68419|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Burdekin Basin.||Of the Wilkie Gray  Group.|||Fossiliferous limestone (calcirudite, calcarenite, and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone.|
27648|Mount Podge Limestone|68420|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Burdekin Basin.||Of the Wilkie Gray  Group.|||Fossiliferous limestone (calcirudite, calcarenite, and lesser calcilutite); minor sandy limestone, calcareous sandstone and mudstone.|
27648|Mount Podge Limestone|68731|5|Briefly described|p177 Fig 3.91, p183, p185 Tb 3.4|Middle Devonian|Lower Devonian|Burdekin Basin. Consists largely of inner shelf carbonates. Rugose corals (Zhen 1995) and conodonts (Talent and Mawson 1994) indicate Emsian to Early Eifelian age.||Of the Wilkie Gray Group.||||
27648|Mount Podge Limestone|72297|5|Briefly described|p728|Middle Devonian|Early Devonian|Quarried mainly for limestone (for cement) at Mount Podge, 80km W of Townsville.|||||Limestone, gypsum.|
30008|Mount Poverty Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
30008|Mount Poverty Granite|43070|2|Defined|p66|Late Permian||Of Cooktown Supersuite.||||||02-JUN-09
30008|Mount Poverty Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Seriate to moderatly porphyritic, biotite granite.||||||
30008|Mount Poverty Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Mount Poverty Suite (Cooktown Supersuite). S-type. Fine- to med.-gr., seriate to mod'l porphyritic tourmaline-muscovite-biotite granite; traces of altered cordierite?; small greisen zones (locally with cassiterite).||||||07-FEB-11
30008|Mount Poverty Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Poverty Suite.|||S-type granitoids.|
36727|Mount Poverty Suite|23423|5|Briefly described|Table 7.1 p240|||Of Collingwood Group.||||||
36727|Mount Poverty Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains Phoenician, Finlayson and Mount Poverty Granites. S-types.||||||07-FEB-11
36727|Mount Poverty Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Mount Poverty, Finlayson, Phoenician Granites.||S-type granitoids.|
23830|Mount Prince Charlie Granophyre|22847|3|Fully described|p 59|Early Permian|Carboniferous|||||||
23830|Mount Prince Charlie Granophyre|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
23830|Mount Prince Charlie Granophyre|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 114. ?I-Type.||||||
23830|Mount Prince Charlie Granophyre|42245|2|Defined|p42|Middle Carboniferous|Permian|||||||
23830|Mount Prince Charlie Granophyre|43093|4|Described|Appendix 1|Early Permian|Carboniferous|Middle Carboniferous to Early Permian.||||||
23830|Mount Prince Charlie Granophyre|43259|4|Described|Appendix 1,p23.|Permian|Carboniferous|||||||
23830|Mount Prince Charlie Granophyre|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
35549|Mount Pring Granite|23162|5|Briefly described|p884||Early Cretaceous|spelt Mt Pring Granite. Age: Biotite 120Ma, K-feldspar 106Ma.||||||
35549|Mount Pring Granite|69594|5|Briefly described|p567, p569, p571 Fig.7.47|Early Cretaceous|Early Cretaceous|Bowen-Mackay region. Geochemical plots.|120.3 +/- 1.3 Ma (K-Ar biotite: Allen et al. 1998)||||Dominantly biotite leucogranite. Miarolitic cavities, pegmatitic patches and microgranophyric textures. Mafic enclaves scarce or absent.|
23831|Mount Pudding Basin Granodiorite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes the Tate Batholith undivided. Geological Province: Georgetown Region.||||||08-JUL-15
23831|Mount Pudding Basin Granodiorite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
23831|Mount Pudding Basin Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 381. I-Type.||||||
23831|Mount Pudding Basin Granodiorite|23624|4|Described|p18|Permian|Carboniferous|Parent: Ootann Supersuite.||||||08-JUL-15
23831|Mount Pudding Basin Granodiorite|42691|5|Briefly described|map legend|Precambrian||Actually spelt Mt Pudding Basin Granodiorite.||||||
23831|Mount Pudding Basin Granodiorite|43110|5|Briefly described|p52|||||||||
23831|Mount Pudding Basin Granodiorite|43259|4|Described|Appendix 1,p43.||Carboniferous|||||||
23831|Mount Pudding Basin Granodiorite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, fine- to medium-grained, even-grained hornblende-biotite granodiorite; with small mafic enclaves.|
23831|Mount Pudding Basin Granodiorite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, fine- to medium-grained, even-grained hornblende-biotite granodiorite; with small mafic enclaves.|
23831|Mount Pudding Basin Granodiorite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Claret Creek Supersuite.|||I-type.|
27846|Mount Rankin Formation|22800|5|Briefly described|p591, p592|||||||||
27846|Mount Rankin Formation|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
27846|Mount Rankin Formation|23161|4|Described|p14 table2b|Early Carboniferous|Early Carboniferous|||||||
27846|Mount Rankin Formation|23430|5|Briefly described|p510|||Drummond Basin Province||||||
27846|Mount Rankin Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Lithic and feldspathic sandstone, conglomerate, mudstone and minor tuff.  Max. thickness: 650m.  Geological Province: Drummond Basin.||||||
27846|Mount Rankin Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
27846|Mount Rankin Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
27846|Mount Rankin Formation|39212|6|Mentioned|p6|||||||||
27846|Mount Rankin Formation|39445|5|Briefly described|Table 6|||||||||
27846|Mount Rankin Formation|40685|5|Briefly described|p400|||||||||
27846|Mount Rankin Formation|40968|4|Described|p276|||||||||
27846|Mount Rankin Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
27846|Mount Rankin Formation|42486|5|Briefly described|p201|||||||||
27846|Mount Rankin Formation|42547|5|Briefly described|Fig.17 P61|||||||||
27846|Mount Rankin Formation|42701|4|Described|p28|||||||||
27846|Mount Rankin Formation|42747|5|Briefly described|p40|||||||||
27846|Mount Rankin Formation|43099|5|Briefly described|p8|||||||||
27846|Mount Rankin Formation|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Anakie Inlier||||overlies Silver Hills Volcanics||23-DEC-11
27846|Mount Rankin Formation|43213|3|Fully described|p88-89, p91|||Mapped by Veevers et al. (1964) as 'Devonian-Carboniferous Volcanics'; this sequence was divided by Olgers (1969) who named the upper sedimentary unit the Mount Rankin beds, which he amended to Mount Rankin Formation in 1972. A type section is proposed in this Report. Deposition in fluvial to lacustrine environments. Correlated with Star of Hope and Ducabrook Formations (Drummond Basin).||||Overlies Silver Hills Volcanics unconformably to disconformably. Is overlain unconformably by Back Creek Group.|Basal clast-supported conglomerate; white, grey and red, flat-laminated siltstone and fine-grained lithofeldspathic to lithic sandstone; minor coarse-grained sandstone, chert, tuff, ignimbrite, and amygdaloidal porphyritic dacite or andesite.|
27846|Mount Rankin Formation|44245|5|Briefly described|Map Legend||Carboniferous|||||||
27846|Mount Rankin Formation|45073|3|Fully described|p42|||||||||
27846|Mount Rankin Formation|60659|4|Described|p14|||Well-bedded feldspathic and lithic quartz sandstone with interbedded mudstone and chert. Disconformably overlies Silver Hills Volcanics; unconformably overlain by Bulgonunna Volcanics.||||||07-FEB-11
27846|Mount Rankin Formation|66084|5|Briefly described|Map legend|Carboniferous|Carboniferous|White and grey siltstone and fine sandstone, minor medium- to very coarse-grained sandstone, chert, granule to pebble conglomerate, rare tuff, ignimbrite, and dacite/ignimbrite.||||||
27846|Mount Rankin Formation|66086|5|Briefly described|Map legend|Carboniferous|Carboniferous|White and grey siltstone and fine sandstone, minor medium- to very coarse-grained sandstone, chert, granule to pebble conglomerate, rare tuff, ignimbrite, and dacite/andesite.||||||
27846|Mount Rankin Formation|68404|5|Briefly described|Map legend|Carboniferous|Carboniferous|Drummond Basin|||||White and grey siltstone and fine sandstone, minor medium to very coarse-grained sandstone, chert, granule to pebble conglomerate, rare tuff, ignimbrite and dacite/andesite.|
27846|Mount Rankin Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Bulliwallah, Ducabrook, Natal and Star of Hope Formations, are all mapped under the symbol, Cd3.||||||
27846|Mount Rankin Formation|68731|5|Briefly described|p191, p191 Fig 3.102, p195|Mississippian|Mississippian|Olgers (1972). Restricted to east of the Anakie Inlier. Crops out in east-central KILCUMMIN, where it is 600 m thick, and as inliers in south-central MOUNT COOLON (Hutton et al. 1999). Detailed lithology discussed.||||Disconformably underlain by the Silver Hills Volcanics.|Comprises clast-supported conglomerate with granule to pebble clasts of felsic volcanics in an arkosic matrix; laminated siltstone with rare ripple laminations and abundant lycopod impressions, and fine, lithofeldspathic to lithic sandstone.|
27846|Mount Rankin Formation|68900|6|Mentioned|p4|Carboniferous|Carboniferous|Drummond Basin.||||||
30204|Mount Razorback Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Mount is Mt. in text. Parent: McBride Basalt Group. Age: <0.27Ma. Geological Province: Georgetown Region.||||||08-JUL-15
30204|Mount Razorback Basalt|23502|5|Briefly described|Map Legend||Quaternary|of McBride Basalt Group.||||||
30204|Mount Razorback Basalt|23619|4|Described|p28 table 1||Pleistocene|Olivine basalt. Of the McBride Basalt Group in the McBride Basalt Province.||||||
30204|Mount Razorback Basalt|23624|4|Described|p27|||Geological Province: McBride Province.||||||08-JUL-15
30204|Mount Razorback Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
30204|Mount Razorback Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
30204|Mount Razorback Basalt|68330|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
30204|Mount Razorback Basalt|68331|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
30204|Mount Razorback Basalt|68576|5|Briefly described|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30204|Mount Razorback Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pleistocene|Pleistocene|McBride Basalt Province.|0.27 Ma|||||
35472|Mount Ridler complex|23215|6|Mentioned|p118|||Written: Mt Ridler complex||||||
81011|Mount Rooper rhyolite|68679|5|Briefly described|p433|Late Triassic|Late Triassic|An informal name for a small outcrop on the mainland near Shute Harbour.|229 Ma (Rb-Sr).||||Fluidal rhyolite and minor breccia.|
69010|Mount Rose Gabbro|61087|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Eidsvold Complex. Medium to dark grey, fine-grained diorite and coarse gabbro; coarse-grained hornblende granodiorite, locally intermingled with the diorite (zones of magma mixing).||||||
69010|Mount Rose Gabbro|64399|5|Briefly described|Map legend|Late Permian|Late Permian|Part of the Edsvold Complex.. Medium to dark grey, fine-grained diorite and coarse gabbro; coarse-grained hornblende granodiorite, locally intermingled with diorite (zones of magma mixing).||||||18-AUG-08
69010|Mount Rose Gabbro|65388|3|Fully described|p290-292, 289, 300|Early Permian|Early Permian|New unit within Eidsvold Complex. Intrudes Nogo beds. In contact with the Harkness Granodiorite, with gabbro appearing older, but may be contemporaneous. K-Ar hornblende age of 250 Ma may be reset. Consists generally of dark grey to black, fine to coarse-grained rocks that range from gabbro or diorite to quartz diorite with equigranular to locally porphyritic textures.||||||
69010|Mount Rose Gabbro|68679|5|Briefly described|p408|Permian|Permian|Auburn Subprovince, New England Orogen.||Eidsvold Complex.|||Dark grey to black, fine- to coarse-grained gabbro or diorite to quartz diorite; intimately mixed with the Harkness Granodiorite at contact.|
74231|Mount Roseby Schist|65387|5|Briefly described|p3 Tb.1, p28-34|Statherian|Statherian|[Status is informal or proposed]. Appears as Mount Roseby schist (informal) in Tb.1 and as Mount Roseby Schist (proposed, IW) on p28. Mount Isa, eastern succession. Hosts the Dugald River Zn-Pb base-metal deposit.|1686 +/- 7 Ma SHRIMP zircon (Carson et al. 2008).||||Includes low-grade, biotite-muscovite laminated metapsammite, intercalated with minor thin ferruginous sandstone and carbonaceous siltstone layers.|
74231|Mount Roseby Schist|67323|5|Briefly described|GIS attrib tbl, p15, p26|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Isa Superbasin. Mary Kathleen Domain, Mount Isa Inlier. Hosts the Dugald River deposit. Is said to include the Dugald River Shale [sic] on p15.||Mount Albert Group.||Time-equivalent of Coocerina and Lady Clayre Formations.|Grey muscovite-biotite-quartz schist (psammopelite) and minor quartzite, calc-silicate granofels and limestone; commonly thin-bedded with abundant poikiloblastic scapolite porphyroblasts, particularly in the north.|
74231|Mount Roseby Schist|68146|5|Briefly described|p200|||Hosts the Dugald River Pb-Zn deposit. Has an identical MDA (Carson et al., 2008) and a broadly similar detrital zircon spectrum to that of the Lady Clayre Dolostone, suggesting a similar clastic provenance.|1686 +/- 7 Ma maximum depositional age.|||||
74231|Mount Roseby Schist|69056|5|Briefly described|p10-11, p55, Time-Space plot sheet|Statherian|Statherian|Comprises rocks previously mapped as Corella Formation. Hosts sediment-hosted stratabound Cu mineralisation (described) and the Dugald River Ag-Pb-Zn deposit.||Upper Mount Albert Group.|Dugald River Shale Member.|Time-equivalent of Coocerina Formation and ?Lady Clayre Dolomite.||
74231|Mount Roseby Schist|69591|5|Briefly described|p43 Fig.2.31, p45, p56|||Mary Kathleen Domain, Mount Isa Province. Some rocks mapped as Corella Formation are assigned to this unit. Part of Gun Supersequence. Deep marine sediments.|1686 +/- 7 Ma (MDA: Carson et al., 2008).||||Grey muscovite-biotite-quartz schist (psammopelite) and minor quartzite, calc-silicate granofels and limestone; commonly thin-bedded with abundant poikiloblastic scapolite porphyroblasts, particularly in the north.|
74231|Mount Roseby Schist|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two facies are separately mapped: marble, mostly impure; and grey to pink, fine-grained, thick to very thick-bedded, massive feldspathic to quartzose sandstone.||Mount Albert Group.|||Grey muscovite-biotite-quartz schist (psammopelite) and minor quartzite, calc-silicate granofels and limestone; abundant poikiloblastic scapolite porphyroblasts.|
74231|Mount Roseby Schist|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Two facies are separately mapped: marble, mostly impure; and grey to pink, fine-grained, thick to very thick-bedded, massive feldspathic to quartzose sandstone.||Mount Albert Group.|||Grey muscovite-biotite-quartz schist (psammopelite) and minor quartzite, calc-silicate granofels and limestone; abundant poikiloblastic scapolite porphyroblasts.|
74231|Mount Roseby Schist|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Four facies are mapped separately.||Mount Albert Group.|Dugald River Shale Member.||Grey muscovite-biotite-quartz schist (psammopelite) and minor quartzite, calc-silicate granofels and limestone; commonly thin-bedded with abundant poikiloblastic scapolite porphyroblasts.|
74231|Mount Roseby Schist|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes two unnamed members: marble, mostly impure; fine-grained, thick to very thick-bedded massive feldspathic to quartzose sandstone.||Mount Albert Group|Includes Dugald River Shale Member and two unnamed members.||Muscovite-biotite-quartz schist and minor quartzite, calc-silicate granofels and limestone; commonly thin-bedded with abundant poikiloblastic scapolite porphyroblasts.|
74231|Mount Roseby Schist|73525|6|Mentioned|p4-5 Fig.2|||Mary Kathleen Domain. Written as Mt Roseby.|||||Carbonaceous siliciclastics.|
74231|Mount Roseby Schist|73529|5|Briefly described|p5|Statherian|Statherian|Calvert Superbasin, late. Deep marine setting.|1686+/-7 Ma maximum depositional age|Mount Albert Group||||
74231|Mount Roseby Schist|73553|6|Mentioned|p8, p228|||Shown as Roseby Schist p8 Fig.1.2.3, part of Mount Albert Group.||||Intruded by Lakeview Dolerite||03-FEB-23
81099|Mount Roundback Granodiorite|69594|5|Briefly described|p567 Fig.7.39|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.||||||
23832|Mount Rous Microgranodiorite|23291|4|Described|p50, p98 Tb. 3.11|Early Carboniferous|Early Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
23832|Mount Rous Microgranodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 42.  I-Type.||||||
23832|Mount Rous Microgranodiorite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23832|Mount Rous Microgranodiorite|40542|6|Mentioned|p97|||||||||
23832|Mount Rous Microgranodiorite|43259|4|Described|Appendix 1,p18.||Carboniferous|Palaeozoic Intrusive No. 42. I-Type.||||||18-JUN-15
23832|Mount Rous Microgranodiorite|43740|4|Described|p27||Carboniferous|||||||
23832|Mount Rous Microgranodiorite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23832|Mount Rous Microgranodiorite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Overlain by Conical Knob Microgranite. Overlies Cook Microgranite.||||||14-MAY-04
23832|Mount Rous Microgranodiorite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Bagstowe Ring Structure, Kennedy Province.|||||Grey to pink, porphyritic biotite-hornblende microgranodiorite.|
23832|Mount Rous Microgranodiorite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Pink, porphyritic hornblende-biotite microgranite.|
68996|Mount Runsome Basalt|61087|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Dark grey, very fine-grained, slightly porphyritic olivine basalt; with ultramafic inclusions, coarse flow banding, columnar jointing.||||||
68996|Mount Runsome Basalt|65388|4|Described|p221-222, 247|Cretaceous|Cretaceous|Small plugs of basalt, Rossmore Station, Rawbelle map sheet. Dated at 72Ma (recalculated) (Green, 1975). Intrudes Crystal Vale Monzogranite.||||||
68996|Mount Runsome Basalt|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran and Gin Gin Basalts; Main Range, Minerva Hills, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
22444|Mount Ryan Quartzite|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Coen Metamorphic Group||||||12-JAN-05
22444|Mount Ryan Quartzite|22781|4|Described|p24|Proterozoic|Proterozoic|Coen Metamorphic Group||||||
22444|Mount Ryan Quartzite|23420|5|Briefly described|p 142 table 4.4|||Possibly the lowest unit in the Coen Metamorphic Group||||||
22444|Mount Ryan Quartzite|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. Forms a 10 x 1 km ridge around Mount Ryan. Possibly the basal unit in the Group. Similar smaller bodies of quartzite interbedded in the Yarraden Schist.||Coen Metamorphic Group.|||Quartzite, minor muscovite and biotite.|
22444|Mount Ryan Quartzite|71792|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Coen Metamorphic Group||Overlies the Goolha Goolha Schist. Overlain by the Yarraden Schist.||
29932|Mount Salmon Volcanics|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kvs].  Rhyolitic and trachytic flows, breccia, ignimbrite and tuff; basalt.||||||
29932|Mount Salmon Volcanics|50209|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
29932|Mount Salmon Volcanics|50213|5|Briefly described|Map legend|Cretaceous|Cretaceous|Rhyolitic and trachytic flows, breccia, ignimbrite and tuff.||||||
29932|Mount Salmon Volcanics|50317|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Trachyte, rhyolite, rhyolitic ignimbrite.||||||09-JUN-04
29932|Mount Salmon Volcanics|60557|5|Briefly described|p19 Fig. 5b, p28|Cretaceous|Cretaceous|Rhyolite and trachyte flows.  Overlie the Alton Downs Basalt. See also p20 Fig. 5c.||||||09-JUN-05
29932|Mount Salmon Volcanics|65388|6|Mentioned|p50|Cretaceous|Cretaceous|Unconformably overlies Youlambie Conglomerate||||||
29932|Mount Salmon Volcanics|65668|5|Briefly described|p2 Tb.1, p25-28|Early Cretaceous|Early Cretaceous|Rockhampton area; New England Orogen. Felsic volcanics, including rhyolite. Age: 119.2 +/- 1.3 Ma (SHRIMP U-Pb zircon), correcting previous suggestions of a Late Cretaceous age from correlation with Mount Hedlow Trachyte.||||||
29932|Mount Salmon Volcanics|68008|3|Fully described|p3, p123, p132, p188, p190-191, p225|Late Cretaceous|Early Cretaceous|See also p250-251, p254-261, p267-268, p393, p485, p493, p530. Simpson (1995), after Kirkegaard et al. (1970). Named after Mount Salmon; they extend 35km to the SE end of Native Cat Range. The type area is between "The Lookout" and the headwaters of Bonley Creek. Forms a dissected plateau and rhyolite benches. Geochemistry detailed and compared with the similar Mount Hedlow Trachyte. Thickness varies up to c.140m. Overlies Dalma Basalt conformably. Repeatedly refers to Dalma Basalt as "forming the base of the Mount Salmon Volcanics", but the authors do not define it as a Member. SHRIMP U-Pb zircon age of a trachyte; overlaps with Wycarbah Volcanics.|119.2 +/- 1.3 Ma (Cross et al., 2009).|||Unconformably overlies Craigilee and Moah Creek beds, Mount Alma and Lorray Formations, Youlambie and Dinner Creek Conglomerates, Rockhampton Group, Ridgelands Granodiorite and Native Cat Andesite.|Trachytic flows, tuffs, breccias and ignimbrite with accompantying rhyolite and basalt. Lithologies well described and illustrated.|
29932|Mount Salmon Volcanics|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit is mapped with Mount Cooper Trachyte under the symbol, Kvs.||||||
29932|Mount Salmon Volcanics|68679|6|Mentioned|p312-313, p347|Cretaceous|Cretaceous|Northern New England Orogen.||||||
29932|Mount Salmon Volcanics|69594|5|Briefly described|p551-552, p559-560, p563|Cretaceous|Cretaceous|Stanwell Basin. Occurs from Mount Salmon ~35km SE to Stanwell. Flooded depositional environment: lacustrine or shallow-marine.|119.2 +/- 1.3 Ma (SHRIMP: Cross et al., 2009).|||Conformably overlies Dalma Basalt. Is overlain by the Stanwell Formation.|Bimodal volcanics: trachyte, rhyolite plugs; trachyte and rhyolite flows and ignimbrite; plagioclase-phyric basalt; rhyolitic and trachytic flows, breccia, ignimbrite and tuff; basalt.|
29932|Mount Salmon Volcanics|69952|6|Mentioned|p75|Late Cretaceous|Late Cretaceous|||||||
29932|Mount Salmon Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|119+/-1.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
29932|Mount Salmon Volcanics|72297|5|Briefly described|p755|||Mount Hay, W of Rockhampton. Source of thunder eggs, agate, chalcedony, agatised rhyolite, quartz crystal, amethyst and smoky quartz.|||||Spherulitic rhyolite flows (containuing diverse silica gemstones), within a complex of acid volcanic plugs, flows and pyroclastics.|
29932|Mount Salmon Volcanics|73450|4|Described|p4, p51-54|Aptian|Aptian|Forms a large dissected plateau NW of Stanwell. May be difficult to distinguish from the Wycarbah Volcanics. Comprises flat-lying to gently dipping extrusive units; individual flows form benches commonly bounded by cliffs. Mostly undivided except for Kvsi (trachyte, rhyolite plugs) and Kvst (trachyte, rhyolite, rhyolitic ignimbrite). Yielded a U-Pb SHRIMP zircon age of 119.2 +/- 1.3 Ma (Cross et al., 2009) and an Ar-Ar anorthoclase age of 119 +/- 2 Ma (Cohen, 2007). Considered as part of a sequence that includes the underlying Dalma Basalt.|119.2 +/- 1.3 Ma U-Pb SHRIMP|||Unconformably underlain by Native Cat Andesite. Conformably underlain by Dalma Basalt.|Fine-grained and porphyritic trachyte flows, highly variable matrix-supported breccias, trachytic and rhyolitic ash and lapilli tuff ignimbrites, and basalt with feldspar phenocrysts.|
77830|Mount Saul Quartz Monzonite|65388|2|Defined|p346-347, 46, 206, 301, 305, 306,340,348|Late Triassic|Late Triassic|Modified after Mount Saul Adamellite.  Now only applies to the south-eastern stock. Intrudes Narayen beds and displays chilled margin. Relationship with Morang Volcanics unclear but may be intrusive. K-Ar dating gave 219+/- 6Ma and 220+/- 6Ma from biotite and hornblende respectively. Greyish to greenish pink, medium-grained biotite-hornblende quartz monzonite in type section.||||||
77830|Mount Saul Quartz Monzonite|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|This unit, as well as the Greencoat Quartz Monzonite and Boolgal Granophyre, are all mapped under the symbol, Rgr.||||||30-SEP-15
77830|Mount Saul Quartz Monzonite|68679|5|Briefly described|p312, p428-429, p441|Late Triassic|Late Triassic|Northern New England Orogen. Is associated with the Rosehall Caldera. May have a genetic relationship involving magma mixing with Morang Volcanics; both are transitional between I-type and A-type.|227-219 Ma (K-Ar and Ar-Ar ages).|||Partly enloses the Morang Volcanics.|Medium-grained, equigranular biotite-hornblende quartz monzonite to monzogranite.|
35182|Mount Scott Granite|23042|4|Described|p84, Fig 2|Cretaceous|Jurassic|||||||
35182|Mount Scott Granite|60473|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Pale pink to dark red or white, medium grained, uneven grained to slightly porphyritic, leucocratic (allanite-hornblende-) biotite monzogranite and syenogranite.||||||
35182|Mount Scott Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35182|Mount Scott Granite|65388|3|Fully described|p414-416, 397, p403 Fig. 135|Cretaceous|Cretaceous|Age uncertain. Outcrop style suggests Cretaceous age, but could be significantly older (late Carboniferous - early Permian). Mainly pink, fine to medium-grained, uneven-grained, leucocratic biotite monzogranite at type locality.||||||
39559|Mount Seaview Igneous Complex|23799|5|Briefly described|p117|||Of Muerray et al (2000, in prep.).  Of the Littlemore Suite.  Geological Province: Yarrol Province.||||||
39559|Mount Seaview Igneous Complex|50197|5|Briefly described|Map Legend|Triassic|Permian|||||||
39559|Mount Seaview Igneous Complex|68008|2|Defined|p330,p333, p369-372, p388,p418,p631,p633|Early Triassic|Permian|New name. These rocks were mapped, but not named, by Dear et al. (1971). Comprises a felsic core, 4 x 2.5 km, completely surrounded by an outer dioritic phase c.2km wide. The type area for the felsic phase is Mount Seaview, after which the Igneous Complex is named, as well as the lower ridge to the SW locally known as Griffiths Hill; and for the dioritic phase, the main access road up the E escarpment of The Tableland. Resistant unit; forms prominent peaks. Geophysics described and modelled. Geochemistry briefly described: is similar to Miriam Vale Granodiorite. The bimodal age distribution may represent crystallisation of the mafic and felsic phases respectively. The combined age is 252.6 +/- 5.3 Ma (Fanning, 2012). Hosts gold deposits (Barmundoo Goldfield).|258 +/- 4.3 Ma and 238.3 +/- 6.9 Ma.|||Intrudes Three Moon and Youlambie Conglomerates, and Rockhampton Group. Is overlain by Precipice Sandstone.|The felsic core is pink, medium-grained, altered, leucocratic biotite granite to granodiorite. The mafic rim is mainly grey, medium- to coarse-grained, augite-biotite-hornblende quartz diorite; cut by andesite dykes. Post-tectonic.|
39559|Mount Seaview Igneous Complex|68679|5|Briefly described|p423, p425|Middle Triassic|Permian|Yarrol belt. An elliptical zoned pluton. Hosts Barmundoo goldfield : stockworks of thin auriferous quartz veins and veins associated with dykes. Bimodal SHRIMP U-Pb zircon ages by Fanning (2012). See also references to the mis-spelt Seaview Igneous Complex (p312, p338).|258.0 +/- 4.3 Ma and 238.3 +/- 6.9 Ma.||||Quartz diorite and quartz gabbro and granite. Felsic core of hornblende-biotite granite and mafic rim of augite-biotite-hornblende quartz diorite and quartz gabbro; granite probably emplaced after quartz diorite.|
39559|Mount Seaview Igneous Complex|71592|5|Briefly described|Appendix A.||||253+/-5.3 Ma (SHRIMP U-Pb zircon).||||Granite.|
36610|Mount Sharples granite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36610|Mount Sharples granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 410.  I-Type.||||||
41940|Mount Shields Granodiorite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Light grey, fine- to medium-grained, equigranular, saccharoidal biotite granodiorite; intruded by andesitic dykes. Part of the Urannah Batholith.||||||16-MAR-06
41940|Mount Shields Granodiorite|65388|2|Defined|p375-376, p135, 362, 364, 365, 399|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Surrounded by Tally Ho Igneous Complex. Probable age given. Intruded by the Whitehorse Granite. Dominantly light grey, mostly fine-grained to locally coarse-grained, saccharoidal, equigranular biotite granodiorite to granite||||||08-SEP-14
41940|Mount Shields Granodiorite|68679|5|Briefly described|p366 Fig.5.56|||Southern Urannah Batholith. Geochemical plots.|||||S-type.|
41940|Mount Shields Granodiorite|73197|6|Mentioned|p470-471|Guadalupian|Late Carboniferous|New England Orogen, northern. Written as Mt Shields Granodiorite on p470.|||||Predominantly I-type granitoids, includes small S-type granitoid phases.|
24404|Mount Sircom Microgranodiorite|23291|4|Described|p48, p98 Tb. 3.11|Permian|Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
24404|Mount Sircom Microgranodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 15. I-Type.||||||
24404|Mount Sircom Microgranodiorite|36216|2|Defined|p213|Carboniferous|Carboniferous|||||||
24404|Mount Sircom Microgranodiorite|39445|5|Briefly described|Table 12|||See also P90||||||
24404|Mount Sircom Microgranodiorite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24404|Mount Sircom Microgranodiorite|40860|5|Briefly described|p116|||||||||
24404|Mount Sircom Microgranodiorite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
24404|Mount Sircom Microgranodiorite|43740|4|Described|p22|||||||||
24404|Mount Sircom Microgranodiorite|50210|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
24404|Mount Sircom Microgranodiorite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Porphyritic hornblende-biotite microgranodiorite.||||||01-JUL-04
24404|Mount Sircom Microgranodiorite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to pink, abundantly porphyritic hornblende-biotite microgranodiorite.|
24404|Mount Sircom Microgranodiorite|68415|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Minimum age possibly Early Permian.|||||Grey to pink, abundantly porphyritic hornblende-biotite microgranodiorite.|
24404|Mount Sircom Microgranodiorite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Cumberland Range Volcanic Group.|||||Hornblende-biotite and biotite microgranite to microtonalite. I-type.|
41782|Mount Spencer Granodiorite|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Greenish grey, medium to coarse grained hornblende granodiorite and tonalite.||||||
41782|Mount Spencer Granodiorite|61917|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Greenish-grey, medium- to coarse-grained hornblende granodiorite and tonalite; intruded by common hornblende-feldspar-phyric andesite and/or dacite dykes.||||||16-MAR-06
41782|Mount Spencer Granodiorite|65388|2|Defined|p376-377, 135, 362, 364, 365,367,375,392|Early Permian|Early Permian|Northern Connors Arch. Southern Urannah Batholith. Intrudes Leura Volcanics. Intruded by Epsom Granodiorite. Other releationships not known. Adjoins Mount Maryvale Granodiorite. Contact may be faulted. Dominantly pale grey to white, mostly medium to coarse-grained, equigranular biotite-hornblende granodiorite wih microdiorite enclaves.||||||
26058|Mount Start Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26058|Mount Start Member|30530|2|Defined|p515|Precambrian|Precambrian|||||||
26058|Mount Start Member|41791|5|Briefly described|p248|||||||||
26058|Mount Start Member|45166|5|Briefly described|p20|||||||||
26058|Mount Start Member|63866|6|Mentioned|p62, p65|||Mitakoodi Anticline.||Marraba Volcanics||||
26058|Mount Start Member|67323|5|Briefly described|GIS attrib tbl; p16|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin||Marraba Volcanics.|||Fine-grained calcareous sandstone, limestone, chert|
26058|Mount Start Member|68732|5|Briefly described|p165|Statherian|Statherian|Of the Myally Supersequence. Sedimentary depositional age.|1774 +/- 4 Ma|||Overlies Cone Creek Volcanic Member. Is overlain by Timberoo Member.|Characterised by siliciclastic and minor carbonate sedimentary rocks.|01-DEC-17
26058|Mount Start Member|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Overlies Cone Creek Metabasalt Member. Is overlain by Timberoo Member.|Fine-grained calcareous sandstone, limestone and chert.|
26058|Mount Start Member|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Overlies Cone Creek Metabasalt Member. Is overlain by Timberoo Member.|Fine-grained calcareous sandstone, limestone and chert.|
26058|Mount Start Member|71799|6|Mentioned|p154|||||Marraba Volcanics||||
26058|Mount Start Member|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Partially equivalent to Cone Creek Metabasalt Member. Overlain by Timberoo Member.|Fine-grained calcareous sandstone, limestone and chert.|
26058|Mount Start Member|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Partially equivalent to Cone Creek Metabasalt Member. Overlain by Timberoo Member.|Fine-grained calcareous sandstone, limestone and chert.|
23833|Mount Storth Granite|23422|5|Briefly described|p219 Table 6.12|||Of Woodstock Suite.||||||
23833|Mount Storth Granite|23431|5|Briefly described|p538|||||||||
23833|Mount Storth Granite|23509|5|Briefly described|Map Legend||Permian|||||||
23833|Mount Storth Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 147. ?A-Type and I-Type.||||||
23833|Mount Storth Granite|23893|5|Briefly described|p21|||||||||
23833|Mount Storth Granite|40607|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
23833|Mount Storth Granite|40954|6|Mentioned|p133|||||||||
23833|Mount Storth Granite|43259|4|Described|Appendix 1,p25.||Permian|||||||
23833|Mount Storth Granite|43935|5|Briefly described|Map Legend||Permian|||||||
23833|Mount Storth Granite|69593|5|Briefly described|p494|Permian|Permian|Townsville region: Lolworth Batholith and Charters Towers Province.|~285-265 Ma (Rienks, 1997).|Woodstock Suite.||||
38251|Mount Stuart Igneous Complex|23422|5|Briefly described|p219 Table 6.12|||Of Woodstock Suite.||||||
38251|Mount Stuart Igneous Complex|69593|5|Briefly described|p494|Permian|Permian|Townsville region: Lolworth Batholith and Charters Towers Province.|~285-265 Ma (Rienks, 1997).|Woodstock Suite.||||
23834|Mount Success Rhyolite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
23834|Mount Success Rhyolite|42750|2|Defined|p46|Permian|Carboniferous|||||||
23834|Mount Success Rhyolite|43259|4|Described|Appendix 1,p5.|Permian|Carboniferous|||||||
23834|Mount Success Rhyolite|43933|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
23834|Mount Success Rhyolite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
23834|Mount Success Rhyolite|71031|5|Briefly described|p3, p56-p57|Early Permian|Late Carboniferous|Charters Towers Province. Age provided is a magmatic crystallisation age. See also the informal Golden Valley rhyolite.|292.4 +/- 1.3 Ma SHRIMP U-Pb|||Overlain by the Big Bend Formation.|Felsic volcanic and subvolcanic igneous rocks including breccia and flow-banded to massive intrusive rhyolite.|
23835|Mount Sugarloaf Igneous Complex|22847|3|Fully described|p 47|Early Devonian|Early Silurian|||||||
23835|Mount Sugarloaf Igneous Complex|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
23835|Mount Sugarloaf Igneous Complex|23513|5|Briefly described|Map legend|Silurian|Ordovician|Palaeozoic Intrusive No. 82. M & I-Type.||||||
23835|Mount Sugarloaf Igneous Complex|42245|2|Defined|p35|Early Devonian|Late Ordovician|||||||
23835|Mount Sugarloaf Igneous Complex|43093|4|Described|Appendix 1|Early Devonian|Early Silurian|||||||
23835|Mount Sugarloaf Igneous Complex|43259|4|Described|Appendix 1,p20.|Early Silurian|Late Ordovician|Late Ordovician to Early Silurian?||||||
23835|Mount Sugarloaf Igneous Complex|43935|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
70383|Mount Takilberan Rhyolite|68421|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic |Shown as equivalent in age to the Grahams Creek Volcanics.|||||Pinkish brown to grey, hornblende-phyric to aphyric, flow-banded and auto-brecciated rhyolite.|
39612|Mount Turner Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
39612|Mount Turner Granite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mostly porphyritic muscovite-biotite granite.||||||05-JUL-04
39612|Mount Turner Granite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province. A variant with sericitic to potassic alteration (related to Carboniferous porphyry systems), commonly associated with breccia, is mapped separately. High K, Th and U radiometric responses.|||||Pale to dark grey, locally foliated, medium-grained, mostly porphyritic muscovite-biotite granite with 10-15 mm tabular K-feldspar phenocrysts.|
39612|Mount Turner Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Pale to dark grey, locally-foliated, medium-grained, mostly porphyritic muscovite-biotite granite with 1-1.5 cm tabular K-feldspar phenocrysts.|
39612|Mount Turner Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith. Large elliptical plutons (mostly 20-75 km2).||Forsayth Supersuite.|||Megacrystic granite.|
41277|Mount Walker Member|50630|5|Briefly described|Map Legend|Devonian|Devonian|Of the Hodgkinson Formation. Arenite, conglomeratic arenite and conglomerate; minor siltstone, mudstone.||||||
41277|Mount Walker Member|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen.|374+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
83292|Mount Walsh Granite|73450|4|Described|p25, p29-35|Norian|Carnian|Referred to as the G4 subdivision of the Mungore Granite, or as 'Mount Walsh granite' by Stephens (1992). Forms a roughly ovoid stock with a N-NW elongation, located south of Biggenden; forms mountainous country (part of the Coast Range) with spectacular outcrops and cliffs. Constitutes the youngest phase of the Mungore Cauldron complex. Truncates volcanic rocks of the Aranbanga Volcanic Group and the main phase of the Mungore Granite. Yielded a U-Pb SHRIMP zircon crystallisation age of 226.5 +/- 1.5 Ma (Cross et al., 2012). Interpreted to have been produced by crystal fractionation from a basaltic parent derived from a primitive mantle source.|226.5 +/- 1.5 Ma U-Pb SHRIMP||Intrudes Gympie Group and Marcella Volcanics, also Aranbanga Volcanic Group and Mungore Granite..||Granite comprising mainly embayed quartz and perthitic K-feldspar, with minor sodic plagioclase, late interstitial Fe-rich biotite, and phenocrystic edenitic amphibole.|16-JUN-22
36105|Mount Wandoo Granodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
36105|Mount Wandoo Granodiorite|24485|5|Briefly described|p54 Tb.8|Late Carboniferous|Late Carboniferous|Intrudes the Nundah Granodiorite||||||
36105|Mount Wandoo Granodiorite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
36105|Mount Wandoo Granodiorite|60425|5|Briefly described|p75 Fig. 15, p76|||Of Retire Suite (Almaden Supersuite). Outcrops west of the Palmerville Fault in the Georgetown Region.||||||07-FEB-11
30164|Mount Warrawee Intrusive Complex|23251|5|Briefly described|Table 5 p34|||Of Cranfield & Scott (1993). SEQld V&P Province.||||||30-NOV-05
30164|Mount Warrawee Intrusive Complex|43100|4|Described|p50|||||||||
24405|Mount Webster Granodiorite|23291|4|Described|p90 Fig. 3.8|Silurian|Silurian|Parent: Mount Webster Supersuite. Geological Province: Georgetown Region.||||||11-MAY-15
24405|Mount Webster Granodiorite|23430|5|Briefly described|p486|||||||||
24405|Mount Webster Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 56. Assumed to be I-Type.||||||
24405|Mount Webster Granodiorite|23619|4|Described|p41 Table 2|||Intrudes Einasleigh Metamorphics. Also see p7. Forms the northern part of Copperfield Batholith. Copperfield Batholith Province.||||||
24405|Mount Webster Granodiorite|39981|2|Defined|p102|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24405|Mount Webster Granodiorite|40542|6|Mentioned|p98|||||||||
24405|Mount Webster Granodiorite|41680|3|Fully described|p119|||||||||
24405|Mount Webster Granodiorite|43113|4|Described|Table 2 p26|||Proterozoic or Silurian to Early Devonian.||||||
24405|Mount Webster Granodiorite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24405|Mount Webster Granodiorite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
24405|Mount Webster Granodiorite|43664|6|Mentioned|p82|||||||||
24405|Mount Webster Granodiorite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
24405|Mount Webster Granodiorite|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Muscovite-biotite granodiorite.||||||
24405|Mount Webster Granodiorite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Pale grey to pinkish grey, locally foliated, equigranular to porphyritic, muscovite-biotite granite and granodiorite; local muscovite granite and pegmatite.|
24405|Mount Webster Granodiorite|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Pale grey to pinkish grey, locally strongly foliated, muscovite-biotite granodiorite.|
24405|Mount Webster Granodiorite|69592|6|Mentioned|p283|||||Mount Webster Supersuite.||||
33894|Mount Webster Supersuite|22533|6|Mentioned|p54|Early Devonian|Silurian|placed in Pama Province||||||
33894|Mount Webster Supersuite|23291|4|Described|p36, p90 Tb. 3.8|Silurian|Silurian|Geological Province: Georgetown Region.||||||08-JUL-15
33894|Mount Webster Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Etheridge Province. This unit, the Dido and White Springs Supersuites, and various ungrouped Silurian plutonic units, are all mapped under the same symbol, Sg.||||||
33894|Mount Webster Supersuite|69592|5|Briefly described|p283-285, p290-291|||Bain et al. (1997); Withnall et al. (2002). Georgetown Inlier. Geochemistry described in some detail. Crustal evolution discussed.|||Mount Webster Granodiorite; Range Creek, Red Knob Granites.||Foliated, muscovite-biotite granodiorite to granite; muscovite-biotite leucogranite; biotite and muscovite-biotite granite. I-type.|
77846|Mount Whacogo Volcanics|65452|5|Briefly described|p5, p6 Fig.2|||Crops out as small remnants on the Rosedale 1:100 000 sheet area. Possibly equivalent to Agnes Water Volcanics. Appears as Mount Whacogu Volcanics in Fig.2.|||||A wide variety of coherent and volcaniclastic facies that range in composition from basalt to rhyolite.|
77846|Mount Whacogo Volcanics|68421|5|Briefly described|Map Legend|Late Triassic|Middle Triassic|Triassic Igneous Province.|||||Feldspar-phyric rhyolitic to dacitic lava and ignimbrite, porphyritic andesite to basalt lava and volcaniclastics, epiclastic sandstone and conglomerate and minor mudstone.|
77846|Mount Whacogo Volcanics|68679|5|Briefly described|p441|Late Triassic|Late Triassic|Agnes Water-Biloela region, northern New England Orogen.|||||Feldspar-phyric rhyolitic to dacitic lava and ignimbrite, porphyritic andesite to basalt lava and volcaniclastics.|
34068|Mount Wright granite|22611|6|Mentioned|P193|||Mount actually spelt Mt||||||
29612|Mount Wyangapinni Suite|43005|5|Briefly described|p215|||||||||
30010|Mount Yates Granodiorite|23511|5|Briefly described|Map Legend||Late Permian|of Yates Supersuite.||||||
30010|Mount Yates Granodiorite|43070|2|Defined|p75|Late Permian||Of Yates Supersuite.||||||03-JUN-09
30010|Mount Yates Granodiorite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Yates Supersuite.  Hornblende-biotite granodiorite.||||||
30010|Mount Yates Granodiorite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Yates Suite (Yates Supersuite). I-type. White to grey, medium-grained, even-grained hornblende-biotite granodiorite; mafic enclaves; hornblende generally scarce; accessory apatite, zircon, ilmenite titanite, allanite, rutile?||||||07-FEB-11
30010|Mount Yates Granodiorite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Yates Supersuite.||||
41587|Mount You You Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Pale pink to pale grey, buff to reddish brown, or cream, fine- to medium-grained, uneven-grained to variably porphyritic biotite monzogranite to syenogranite; minor hornblende-biotite monzogranite, aplitic leucogranite, gabbro.||||||11-DEC-07
41587|Mount You You Granite|63748|3|Fully described|p30|Early Triassic|Permian|Of Mount You You Suite. Previously mapped as part of Ruby Creek Granite (Robertson 1974). Pale grey to pale pink, fine- to medium-grained, moderately porphyritic, leucocratic biotite syenogranite. High K, I-type. See also p27 Fig.27.||||||07-FEB-11
41587|Mount You You Granite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, as well as Ballandean, Clare Hills, Fairleigh, Herries, Jibbinbar, Mount Bullaganang and Palgrave Granites; Boxwell and Greymare Granodiorites; are all mapped under the symbol, Pgn.||||||
41587|Mount You You Granite|68679|4|Described|p445, p454-456|Permian|Permian|Northern New England Batholith. Had been mapped as Ruby Creek Granite (Robertson, 1974); differences listed. ~14 km2. A composite pluton; texturally and mineralogically heterogeneous. Moderately evolved, high-K, I-type.|294.0 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Mount You You Suite.||Intrudes Texas beds.|Fine- to medium-grained, variably porphyritic to seriate, leucocratic biotite monzogranite to syenogranite; minor hornblende-biotite monzogranite; locally granophyric, miarolitic; associated with pods and lenses of gabbro.|
41587|Mount You You Granite|68901|6|Mentioned|p8 Fig. iii|Early Permian|Early Permian|||||||27-SEP-18
41587|Mount You You Granite|69639|5|Briefly described|p44, p220|Sakmarian|Sakmarian|New England Orogen.|294 +/- 2.9 Ma (Rosenbaum et al, 2012)|Mount You You Supersuite||||
41587|Mount You You Granite|70373|6|Mentioned|p790, p791|Early Permian|Early Permian||~294 Ma|||||
41587|Mount You You Granite|71628|5|Briefly described|p5: 1, 7|||Donchak et al. (2007).||Mount You You Supersuite.||||
82598|Mount You You Leucogranite|71628|4|Described|p5: 1, 4, 7-9; p19-145|Permian|Permian|Originally the Mount You You Granite (Donchak et al., 2007). Renamed in this study. Named after Mount You You. Crops out over ~14 km2 about 5 km W of Pikedale as scattered boulders, tors, whalebacks and pavements in undulating to low hilly country. Geochemistry described.|294.0 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Mount Bullaganang Supersuite.||Intrudes Texas beds. Is faulted against Pikedale beds. Encloses a parallel, Pike Creek Dolerite, dyke: relationship unknown.|Pale pink to pale grey, buff to reddish brown, or cream, fine- to medium-grained, inequigranular to porphyritic biotite monzogranite to syenogranite; minor hornblende-biotite monzogranite and aplitic leucogranite. I-type.|
73979|Mount You You Suite|63748|5|Briefly described|p30|Early Triassic|Permian|Of Mount You You Supersuite. Includes Mount You You Granite.||||||07-FEB-11
73979|Mount You You Suite|68679|5|Briefly described|p454, p457-459|Permian|Late Carboniferous|Northern New England Batholith. Comprises several small stocks of leucogranite. Geochemistry described.|~298 Ma.|Stanthorpe Supersuite.|Mount You You, Jibbinbar, Treverton Granites.|||
73979|Mount You You Suite|71628|5|Briefly described|p5: 2, 7, 10|||Donchak et al. (2007) included this unit within the Mount You You Supersuite. Brown et al. (2014) placed this Suite in the Bullaganang Supersuite. In this study, this Suite is placed in the Mount Bullaganang Supersuite.||Mount Bullaganang Supersuite.|Jibbinbar Leucosyenogranite; Mount You You, Treverton Leucogranites.|||
73980|Mount You You Supersuite|63748|5|Briefly described|p30|Early Triassic|Permian|Includes Mount You You Suite.||||||07-FEB-11
73980|Mount You You Supersuite|65668|6|Mentioned|p1|||Includes the Jibbinbar Granite (Donchak et al., 2007).||||||
73980|Mount You You Supersuite|69639|5|Briefly described|p44, p220|||New England Orogen.|||Includes the Mount You You Granite and the Jibbinbar Granite.|||
73980|Mount You You Supersuite|70876|5|Briefly described|p80|Early Permian|Early Permian|Donchak et al (2013) incorporated this Supersuite into the Stanthorpe Supersuite; the authors of this volume however, note significant age ranges of the incorporated Supersuites and thus suggest this issue be revisited.|c. 298 Ma (Donchak et al, 2013)|||||
73980|Mount You You Supersuite|71628|5|Briefly described|p5: 1-2, 7, 10|||Donchak et al. (2007) included the Mount You You Suite in this unit. Brown et al. (2014) placed that Suite in the Bullaganang Supersuite. Now (?this study) replaced by the Mount Bullaganang Supersuite.|||Jibbinbar Leucosyenogranite and Mount You You Leucogranite.|||
36241|Mountain Camp Granite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|Intrudes Mount Cardwell, Sandy Tate(?) Granites; intruded by Branch Creek rhyolite. Geological Province: Georgetown Region.||||||08-JUL-15
36241|Mountain Camp Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36241|Mountain Camp Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 370. I-Type.||||||
36241|Mountain Camp Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36241|Mountain Camp Granite|23624|4|Described|p12|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||03-JUL-15
36241|Mountain Camp Granite|60425|5|Briefly described|p280-1 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. (no description included).||||||07-FEB-11
36241|Mountain Camp Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium- to coarse-grained, porphyritic biotite monzogranite and granodiorite. Intensely altered, silicified, porphyritic monzogranite and granodiorite is/are mapped separately.|
36241|Mountain Camp Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to cream, medium- to coarse-grained, porphyritic biotite monzogranite and granodiorite. Intensely altered, silicified, porphyritic monzogranite and granodiorite is/are mapped separately.|
41786|Mountain View Volcanics|60445|5|Briefly described|p5, p6|||Of Connors Volcanic Group. Consists of mafic to intermediate volcanics, massive polymictic conglomerate, minor felsic volcanics, well bedded labile sandstone and siltstone. Conformably overlain by Carmila beds.||||||
41786|Mountain View Volcanics|60473|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Andesitic to rhyolitic lava flows and volcaniclastic rocks, basalt and andesite; minor dacite to rhyolite.||||||
41786|Mountain View Volcanics|60475|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Andesitic to rhyolitic flows and volcaniclastic rocks, including crystal rich volcanic sandstone, volcanic breccia, conglomerate and crystal rich ignimbrite.||||||
41786|Mountain View Volcanics|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Heterogeneous assemblage of andesitic to rhyolitic flows and volcaniclastic rocks, including crystal rich volcanic sandstone, volcanic breccia and conglomerate and crystal rich ignimbrite.||||||29-SEP-04
41786|Mountain View Volcanics|60480|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Heterogeneous assemblage of andesitic to rhyolitic flows and volcaniclastic rocks, including crystal rich volcanic sandstone, volcanic breccia and conglomerate and crystal rich ignimbrite.||||||
41786|Mountain View Volcanics|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
41786|Mountain View Volcanics|61035|5|Briefly described|p6|Carboniferous|Early Carboniferous|Of the Conners Volcanic Group. Age: ~330Ma (SHRIMP). Consists of basaltic to rhyolitic lava flows and volcaniclastic rocks. Geological Province: Connors Sudprovince.||||||07-FEB-11
41786|Mountain View Volcanics|61916|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Heterogenous assemblage of andesitic to rhyolitic lava flows and volcaniclastic rocks (including crystal-rich ignimbrite, volcanic breccia and conglomerate, and feldspathic sandstone).||||||
41786|Mountain View Volcanics|61917|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Heterogenous assemblage of andesitic to rhyolite flows and volcaniclastic rock, inc. crystal-rich volcanic sandstone, volcanic breccia and conglom; grey,greenish-grey, vey fine-gr. to fine-gr., porphyritic to locally aphyric basalt and andesite.||||||16-MAR-06
41786|Mountain View Volcanics|65388|4|Described|p89-94; p90, 59, 64, 68, 74, 85, 86|Early Carboniferous|Late Devonian|Of Connors Volcanic Group, Connors Arch. Previously Mountain View beds of Hutton and others (1999a) but now extended. Intruded by Burwood Complex, Olympus Granite, Toobier Granite. Overlain by Whelan Creek Volcanics, Leura Volcanics, Carmila beds, Collaroy Volcanics. Presumed to be overlain by Broadsound Range Volcanics. No type section. Killarney-Burwood Rd designated as reference area. No direct date. Mainly very fine-grained to fine-grained, porphyritic basalt and andesite. Minor rock types include volcanic breccia, sandstone, lithics-rich dacitic ignimbrite, volcanic breccia, porphyritic rhyolite (lava). See also p104, 109, 110, 135, 136, 149, 358, 360, 362, 393, 441, 443, 447.||||||
41786|Mountain View Volcanics|68679|4|Described|p353, p355-356|Mississippian|Mississippian|Connors-Auburn Province. Crops out as a belt ~110km long and up to 25km wide, from near Koumala and Carmila through the eastern Connors Range. Subaerial eruptions; mass flows, fluvial traction currents, and probable lacustrine deposits. Not directly dated; may be older than Mississippian. Presumed hiatus of c.20m.y. before overlying unit deposited.|<328 +/- 4Ma (age of intrusion).|Connors Volcanic Group.||Is overlain by the Broadsound Range Volcanics and Whelan Creek Volcanics. Is intruded by the Burwood Complex.|Mainly porphyritic basalt and andesite; minor volcanic breccia and sandstone, lithic dacitic ignimbrite and porphyritic rhyolite lava; also massive pebble to cobble conglomerate, labile sandstone, siltstone and shale.|
33436|Mountefontein Metamorphics|23799|3|Fully described|p23, p15 Tb. 1|Late Carboniferous|Carboniferous|Concordant with the Chahpingah Meta-Igneous Complex.  Intruded by various phases of Boondooma Igneous Complex.  Geological Province: Yarraman Subprovince (Wandilla Province).||||||
33436|Mountefontein Metamorphics|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
33436|Mountefontein Metamorphics|50384|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: Yarraman Subprovince.||||||
33436|Mountefontein Metamorphics|60371|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: Yarraman Subprovince. Thinly-interlayered biotite gneiss and fine schist.||||||
33436|Mountefontein Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Yarraman Subprovince. This unit, as well as Bjelke Petersen and Maronghi Creek beds, Fifer Creek and Sugarloaf Metamorphics, and unnamed sedimentary units, are all mapped under the symbol, DCym.||||||
33436|Mountefontein Metamorphics|68679|5|Briefly described|p321-324|Late Carboniferous|Late Carboniferous|Cranfield et al. (2001). Yarraman Subprovince, Wandilla Province, northern New England Orogen. Occupies a small (12 km2) discrete area 30km W of Kingaroy. An extensional complex.||||Concordant with (probably intruded and enclosed by) Chahpingah Meta-Igneous Complex.|Mainly thinly interlayered biotite gneiss and fine schist, intruded by scattered biotite-leucogranite sills and migmatitic veins. Sporadic, thick belts of thinly banded hematitic metachert.|
25301|Mowbray Creek granite|39283|4|Described|p419|||Petrology||||||
25301|Mowbray Creek granite|39997|6|Mentioned|p165|||||||||
30191|Mrs Watsons Bay Microgranite|43111|2|Defined|p52|Late Permian||||||||
30191|Mrs Watsons Bay Microgranite|60425|5|Briefly described|p272 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. No suite assigned. S-type.White, cream or brown (altered) mainly fine-gr., equigran to slightly porph. tourmaline-biotite-muscovite leucogranite with irregular pegmatite zones; forms dykes, lenses, subhorizontal sheets, and pods.||||||07-FEB-11
30191|Mrs Watsons Bay Microgranite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|||S-type granitoids.|
77831|Mueller Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Sandstone, conglomerate.|
77831|Mueller Formation|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott and Poodyea Formations; Austral Downs, Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
26062|Muggleton Formation|13516|6|Mentioned|p145 fig 3, p147 fig 5|Late Permian|Late Permian|From Roma Shelf, Bowen Basin. Age: APP5004||||||
26062|Muggleton Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26062|Muggleton Formation|24069|5|Briefly described|p284|Permian|Permian|Geological Province: Surat Basin.||||||
26062|Muggleton Formation|24077|5|Briefly described|p410 Tb. 3|Late Permian|Early Permian|Includes the Lorelle Sandstone Member.  Grey shale siltstone and sandstone, few coquinite and tuff bands and coal seams.  Max. thickness: 148m.  Geological Province: Bowen Basin.||||||
26062|Muggleton Formation|29391|6|Mentioned|Table 4|||See p19.||||||17-NOV-15
26062|Muggleton Formation|29721|6|Mentioned|Table 269|||||||||
26062|Muggleton Formation|32578|2|Defined|p354|Late Permian|Early Permian|Late Early ? to Late Perm.||||||
26062|Muggleton Formation|36739|6|Mentioned|p22|||||||||
26062|Muggleton Formation|37065|6|Mentioned|p30|||||||||
26062|Muggleton Formation|39445|5|Briefly described|Table 8|||||||||
26062|Muggleton Formation|39494|6|Mentioned|Fig.5|||||||||
26062|Muggleton Formation|40030|6|Mentioned|Fig.5|||||||||
26062|Muggleton Formation|40544|6|Mentioned|Fig.6|||||||||
26062|Muggleton Formation|41247|6|Mentioned|Fig.7|||||||||
26062|Muggleton Formation|42250|6|Mentioned|Fig.3 P30|||||||||
26062|Muggleton Formation|43000|6|Mentioned|p111|||||||||
26062|Muggleton Formation|45110|4|Described|Table 16|||See also p52 and Table 13.||||||17-NOV-15
26062|Muggleton Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
26062|Muggleton Formation|63713|5|Briefly described|p1507 Fig.2, p1528|Roadian|Kungurian|Roma Shelf, Bowen Basin. Shown in Fig.16 as Upper and Lower Muggleton Formation separated by Lorelle Sandstone Member. Well-log correlation.|||Includes Lorelle Sandstone Member.|Is overlain by Tinowon Formation.||
26062|Muggleton Formation|64856|4|Described|p42, p59, p63-65|Late Permian|Late Permian|Paten and Groves (1974). Bowen Basin. Includes Lorelle Sandstone Member. Unconformably overlies Timbury Hills Formation or Combarngo Volcanics. Underlies Tinowon Fm. Correlated with Banana Fm. Age from palynoflora (APP5). Shale, siltsone, sandstone, minor coal, tuff. 197m thick.| | ||||29-NOV-17
26062|Muggleton Formation|64857|5|Briefly described|p119-121, p113 Fig.3|Late Permian|Late Permian|Western Bowen Basin. Mudstone interval grading up into the Tinowon Formation in the west part of the southern Taroom Trough and the lower coal interval of the Burunga Formation in the south.||||||
26062|Muggleton Formation|64858|6|Mentioned|p190, p180 Fig.2|Late Permian|Late Permian|Age middle Late Permian.||||||30-NOV-09
26062|Muggleton Formation|64859|5|Briefly described|p196, 225|Permian|Permian|Mainly marine mudstones. Gas source rocks.||||||
26062|Muggleton Formation|65115|6|Mentioned|p414, 416|Kazanian|Ufimian|Roma Shelf. Equivalent to Banana Formation, Taroom Trough.||||||
26062|Muggleton Formation|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
26062|Muggleton Formation|67402|5|Briefly described|p21, p48 tbl BWS1|Capitanian|Capitanian|Bowen Basin. Deposited in a fluvial to fluvial-deltaic environment.||||Overlain by the Black Alley Shale. Unconformably overlies the Arbroath beds.|Shale, siltstone, quartzose sandstone, coal and tuff.|
26062|Muggleton Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Tinowon Formation /Wallabella CM. Underlain by Combarngo volcanics.||
26062|Muggleton Formation|68679|5|Briefly described|p377, p381-382|Permian|Permian|Paten and Groves (1974). Bowen Basin. 197m thick. Nearshore to delta deposits. Isotopic dating shows this Formation is older than the Catherine Sandstone.|||Lorelle Sandstone Member.|Is overlain by Tinowon Formation. Correlates with the Barfield Formation.|Shale, siltstone, sandstone (fine- to coarse-grained, locally conglomeratic, quartzose, feldspathic), and minor coal and tuff; marine fossils present.|
26062|Muggleton Formation|70878|5|Briefly described|p720 Fig.15|Permian|Permian|Bowen Basin.||||Is overlain by Tinowon Formation.||
26062|Muggleton Formation|72297|6|Mentioned|p744|||Southern Bowen Basin. Sandstones in this unit are hydrocarbon reservoirs.||||||
26062|Muggleton Formation|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Roma Shelf, Western Bowen Basin.||||Is overlain by Tinowon Formation.||
22462|Muirson Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
22462|Muirson Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
22462|Muirson Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
22462|Muirson Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V131. I-Type.||||||
22462|Muirson Rhyolite|23616|5|Briefly described|Table 3 p49||Carboniferous|Of Boonmoo Volcanic Subgroup||||||
22462|Muirson Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
22462|Muirson Rhyolite|43259|4|Described|Appendix 1,p14.||Late Carboniferous|Of Boonmoo Volcanic Subgroup.||||||03-JUN-09
22462|Muirson Rhyolite|43567|5|Briefly described|Table 2,p400|||||||||
22462|Muirson Rhyolite|43626|2|Defined|p23||Late Carboniferous|younger than 306+/-3 Ma older than 304+/- 4 Ma||||||
22462|Muirson Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22462|Muirson Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
22462|Muirson Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A "geophysical subdivision" of this unit, described as a probable variant, is mapped separately.||Unit in Boonmoo Volcanic Subgroup.|||Dark to very dark grey, or bluish to greenish grey, moderately to very crystal rich, hornblende-biotite rhyolitic ignimbrite; with quartz < 8 mm and fiamme up to 10 cm long.|
22462|Muirson Rhyolite|68576|5|Briefly described|Q_11: p11-12|||Not dated, but the overlying unit is 308 +/- 8 Ma.||Basal Boonmoo Volcanic Subgroup.||Is overlain by Hopscotch Rhyolite.|Green, very crystal-rich, lithic-poor rhyolitic ignimbrite; less common mafic mineral clasts (biotite and hornblende). Local fiamme up to 10 cm long.|
29334|Muldiva Quartz Monzodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
29334|Muldiva Quartz Monzodiorite|23616|6|Mentioned|p71 Fig 13|||||||||
29334|Muldiva Quartz Monzodiorite|43060|5|Briefly described|Table 6|||||||||
29334|Muldiva Quartz Monzodiorite|43083|6|Mentioned|p109 tb. 7|||Not assigned to any suite/supersuite.||||||17-JUN-09
29334|Muldiva Quartz Monzodiorite|43087|2|Defined|p59|Late Carboniferous|Late Carboniferous|New name. Hussey (1989, p33) used the term 'Muldiva Granodiorite' (informal name) to delineate part of the unit. Irregular pluton (~5 km2). Type locality proposed. Massive and unmetamorphosed. Age: most probably Late Carbonfierous.||||Forms extensive net-veined complexes with Quaker Granite.|Predominantly grey to dark-grey, fine to medium-grained, even-grained to slightly porphyritic quartz monzodiorite; rare rounded quartz aggregates.|01-APR-15
29334|Muldiva Quartz Monzodiorite|43259|4|Described|Appendix 1,p39.||Carboniferous|||||||
29334|Muldiva Quartz Monzodiorite|60425|4|Described|p75 Fig. 15, p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Retire Suite (Almaden Supersuite). Grey to dark grey, fine- to medium-grained, even-grained to slightly porphyritic biotite-hornblende quartz monzodiorite; forms extensive net-veined complex with the Quaker Granite. I-type.||||||07-FEB-11
23844|Mulgrave Formation|23032|6|Mentioned|p17||Early Ordovician|||||||
23844|Mulgrave Formation|23039|6|Mentioned|p170||Paleozoic|||||||07-NOV-08
23844|Mulgrave Formation|23076|5|Briefly described|p724|Ordovician|Ordovician|||||||
23844|Mulgrave Formation|23422|5|Briefly described|Plate 7.3|Early Carboniferous|Early Ordovician|||||||
23844|Mulgrave Formation|23423|4|Described|p303 Table 7.2|Ordovician|Early Ordovician|Locally overlain by Mountain Creek Conglomerate and Van Dyke Litharenite unconformably. Also see p229-231. Overlying unit Quadroy Conglomerate. Hodgkinson Province.||||||
23844|Mulgrave Formation|23424|6|Mentioned|p344|||Correlate of Broken River Group units. Hodgkinson Province.||||||
23844|Mulgrave Formation|23430|4|Described|471-473p|||Hodgkinson Province.||||||
23844|Mulgrave Formation|23431|5|Briefly described|p539|||||||||
23844|Mulgrave Formation|23500|5|Briefly described|Map legend|||Age: Early Ordovician?||||||
23844|Mulgrave Formation|23511|5|Briefly described|Map Legend||Early Ordovician|||||||
23844|Mulgrave Formation|23616|4|Described|Table 1C p15, p29||Early Ordovician|Faulted against Dargalong Metamorphics. Unconformably underlies or is faulted against the Silurian-Devonian Chillagoe Formation. Age: Early to Middle Ordovician; unconformably overlain by Late Ordovician limestones which provide upper age limit for fm.||||||
23844|Mulgrave Formation|23713|5|Briefly described|p13||Ordovician|Hodgkinson Province.||||||
23844|Mulgrave Formation|24086|5|Briefly described|p312 Fig. 1|Ordovician|Ordovician|||||||
23844|Mulgrave Formation|24213|5|Briefly described|p776 Fig. 1|Early Devonian|Early Silurian|||||||
23844|Mulgrave Formation|24485|5|Briefly described|p5||Late Ordovician|Overlying Unit: Quadroy Conglomerate. Geological Province: Hodgkinson Province||||||
23844|Mulgrave Formation|24486|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|||||||
23844|Mulgrave Formation|24487|5|Briefly described|Map legend|||||||||
23844|Mulgrave Formation|40892|5|Briefly described|p74|||||||||
23844|Mulgrave Formation|41569|6|Mentioned|p71|||||||||
23844|Mulgrave Formation|41775|6|Mentioned|p71|||||||||
23844|Mulgrave Formation|41824|6|Mentioned|p201|||||||||
23844|Mulgrave Formation|41825|6|Mentioned|p204|||||||||
23844|Mulgrave Formation|42113|6|Mentioned|p259|||||||||
23844|Mulgrave Formation|42304|6|Mentioned|p5|||||||||
23844|Mulgrave Formation|42500|5|Briefly described|p11, p15|||||||||
23844|Mulgrave Formation|42620|1|Redefined|p51||Late Ordovician|Redefinition of Fawckner's(1981) Mulgrave Fm.||||||
23844|Mulgrave Formation|42658|6|Mentioned|p16|||||||||
23844|Mulgrave Formation|42772|5|Briefly described|p16, Fig.18|||||||||
23844|Mulgrave Formation|43060|5|Briefly described|p37,Table 1c|Ordovician|Early Ordovician|||||||
23844|Mulgrave Formation|43083|3|Fully described|p30, p31 Tb. 2|||Geological province: Hodgkinson Province. Probable Early to Middle Ordovician age. mainly fine- to medium-grained quartzose arenite.||||||17-JUN-09
23844|Mulgrave Formation|43213|6|Mentioned|p66|Ordovician|Ordovician|Quartzose flysch sediments, preserved as thrust slices.||||||
23844|Mulgrave Formation|43254|5|Briefly described|map legend||Ordovician|of Hodgkinson Province. Probably Early Ordovician.||||||
23844|Mulgrave Formation|43285|5|Briefly described|Map Legend|||age Early Ordovician?||||||
23844|Mulgrave Formation|43625|4|Described|p19,20|||Age: ?Early Ordovician||||||
23844|Mulgrave Formation|43665|6|Mentioned|p21|Devonian|Ordovician|||||||
23844|Mulgrave Formation|44246|5|Briefly described|Map Legend||Ordovician|||||||
23844|Mulgrave Formation|60357|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Geological Province: Hodgkinson Province.||||||
23844|Mulgrave Formation|60358|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Geological Province: Hodgkinson Province.||||||18-AUG-04
23844|Mulgrave Formation|60425|3|Fully described|p5, p18 Tb. 1, p18-20|Early Ordovician|Early Ordovician|Faulted against/locally unconformable below Quadroy Conglom; also faulted against Chillagoe Fm. Max.thickness: <1000m. Geol.prov: Hodgkinson Province. Quartzose arenite with subordinate interbedded metabasalt, mudstone, siltstone, shale; unfossiliferous||||||07-FEB-11
23844|Mulgrave Formation|62371|5|Briefly described|p470 Fig.1|Early Devonian|Ordovician|Geological Province: Hodgkinson Province. See also p472 Fig.3||||||
23844|Mulgrave Formation|63140|4|Described|p569-583.|Middle Ordovician|Early Ordovician|Deposition in passive continental margin setting. Major, trace and REE geochemistry are detailed. Sub-continental lithosphere sourced basalt.|c.555 Ma.|||Overlain unconformably by Mountain Creek Conglomerate and Van Dyke Litharenite.|Basalt and basaltic andesite, interspersed with marine quartzose sedimentary rocks and limestones.|
23844|Mulgrave Formation|63154|5|Briefly described|p281 Fig. 3|Ordovician|Ordovician|Age: ~490-455Ma. Geological province: Hodgkinson Province. Sedimentary.||||||11-APR-07
23844|Mulgrave Formation|67848|5|Briefly described|p16.|||Western margin of Hodgkinson Province. Undated; possibly Ordovician. Comparable rock assemblage to the arc assemblage and Wairuna Formation of Broken River Province. Includes basalt of island arc affinity.||||||
23844|Mulgrave Formation|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Mount Windsor Subprovince. This unit, as well as Mountain Creek and Quadroy Conglomerates, and Van Dyke Litharenite, are all mapped under the symbol, Om.||||||
23844|Mulgrave Formation|68576|6|Mentioned|Q_11: p16|||||||||
23844|Mulgrave Formation|69030|6|Mentioned|p6|Ordovician|Ordovician|Chillagoe Subprovince, Hodgkinson Province.||||||
23844|Mulgrave Formation|69079|6|Mentioned|p3-4|Early Ordovician|Early Ordovician|Hodgkinson Province.||||||
23844|Mulgrave Formation|69592|5|Briefly described|p230-233, p245, p297, p304|Ordovician|Ordovician|Fawckner (1981); Bultitude and Donchak (1992). Chillagoe Subprovince, Hodgkinson Province. Occurs as several discontinuous belts from ~100m to ~3.5 km wide, from Mungana area to Mount Mulgrave; forms ridges separating recessive belts of Van Dyke Litharenite (both units referred to as Thomson Orogen strata). Deep-marine density current sands, and pelagic and hemipelagic cherts and mudstones. Youngs mainly to the west. Source of most clasts in Mountain Creek Conglomerate. Age is unconstrained; based on similarities with other units.||||Structurally intercalated with Chillagoe Formation. Is faulted against and structurally intercalated with Mountain Creek Conglomerate.|Mainly quartz-rich sandstone, interbedded with subordinate mudstone, siltstone, shale; local intercalations of chert, hematitic mudstone and mafic volcanic rocks; numerous depositional structures listed. Interstitial chlorite, quartz veinlets common.|
23844|Mulgrave Formation|70207|4|Described|p1, p11, p74, p94-100|Silurian|Silurian|Thomson Orogen. Crops out as bouldery rubble. Considered Ordovician because of similarity with Judea Formation, and spatial association with Mountain Creek Conglomerate. Maximum depositional age; significantly younger than adjacent Mountain Creek Conglomerate and other Thomson Orogen units; the sample is possibly from the younger Chillagoe Formation.|423.5 +/- 9.3 Ma (Kositcin et al., 2015).|||Structurally intercalated with Chillagoe Formation.|Dominated by fine-grained, quartz-rich sandstone and subordinate chert, hematitic mudstone and metabasalt.|
23844|Mulgrave Formation|71031|4|Described|p4-p6, p13, p70-p72|Devonian|Devonian|Thomson Orogen, Hodgkinson Province. Interpreted as probably Devonian by Fawckner (1981) subsequent worker (e.g. Bultitude et al, 1993, 1996; Domagala, 1997; Henderson and Donchak, 2013) regarded it to be most probably Lower to early Upper Ordovician due to its similarity with the Lower Ordovician Judea Formation of the Broken River Province (Withnall and Lang, 1990) and its position adjacent to the late Upper Ordovician Mountain Creek Conglomerate. U-Pb zircon SHRIMP dating in this volume supports Fawckners original interpretation and includes two additional ages: 421.5 +/- 4.3 Ma and 471.4 +/- 2.8 Ma (Cohen et al., 2015). See also p75-p77, p79, p81, p85, p86-p87.|423.5 +/- 9.3 Ma (Kositicin et al 2015a; max dep)|||Conformably overlies the Chillagoe Formation.|Quartzose sandstone.|
23844|Mulgrave Formation|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen.|424+/-9.3 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
23844|Mulgrave Formation|72983|6|Mentioned|p15|Carboniferous?|Ordovician|||||||
23844|Mulgrave Formation|73595|6|Mentioned|p1134|||Hodgkinson Province, Mossman Orogen.||||||
30197|Mulindie Granite|23291|5|Briefly described|p102 Tb. 3.13|Early Permian|Late Carboniferous|Parent: Mulindie Suite. Intrudes Tate Batholith undivided. Age: ~282 Ma (Black, 1978). Geological Province: Georgetown Region.||||||08-JUL-15
30197|Mulindie Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
30197|Mulindie Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 371. I-Type.||||||
30197|Mulindie Granite|23616|5|Briefly described|p99 Appendix 2||Permian|Of Ootann Supersuite.||||||
30197|Mulindie Granite|23624|4|Described|p14|Permian|Carboniferous|Parent: Ootann Supersuite.||||||17-DEC-13
30197|Mulindie Granite|43113|6|Mentioned|Table 1 p23|||Variation on reserved name Mulindie Adamellite. Misspelling of Mullindie Granite?||||||
30197|Mulindie Granite|43253|5|Briefly described|map legend||Carboniferous|||||||
30197|Mulindie Granite|43259|4|Described|Appendix 1,p42.||Carboniferous|||||||
30197|Mulindie Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink or red, medium- to coarse-grained, even-grained biotite monzogranite.|
30197|Mulindie Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink or red, medium- to coarse-grained, even-grained biotite monzogranite.|
37887|Mulindie Suite|23291|5|Briefly described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
69878|Munbooree beds|61761|6|Mentioned|p4|||Geological Province: Philpott Block, Gamilaroi terrane.||||||07-FEB-11
69878|Munbooree beds|64398|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Siltstone, arenite, conglomerate, limestone.||||||
69878|Munbooree beds|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Marble Waterhole, Craigilee, Calliope and Dunollie beds, and the Pumpkin Hut Mudstone, are all mapped under the symbol, Dc.||||||
69878|Munbooree beds|68679|5|Briefly described|p312-313, p317, p401|Middle Devonian|Late Silurian|Withnall (1972); Whitaker, Murphy and Rollason (1974). Originally restricted to Toondahra Creek and Big Oaky Creek areas; extended to include a belt of Devonian rocks N to Boyne River by Withnall and Turner (2007). Philpott Subprovince, northern New England Orogen.||||Is overlain conformably by Dunollie beds.|Siliceous siltstone, feldspatholithic sandstone and conglomerate containing minor limestone boulders and pebbles; the conglomerate has volcanic clasts and grades into the volcaniclastic rocks of the overlying unit.|
35203|Munbura Diorite|23042|5|Briefly described|Fig 2||Cretaceous|||||||
35203|Munbura Diorite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35203|Munbura Diorite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Dark greenish- grey, fine- to medium-grained, equigranular diorite and microdiorite and some dark grey to black, coarse-grained, equigranular gabbro. Intrudes Mountain View Volcanics and Carmila beds.||||||
35203|Munbura Diorite|65388|2|Defined|p416-417, 415, p403 Fig. 135, p419|Cretaceous|Cretaceous|Intrudes and has hornfelsed Carmila beds. Likely age given.Dominantly medium-dark grey, fine to medium-grained, equigranular diorite or gabbro.||||||
27850|Muncon Volcanics|9194|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Andesite, trachyte, agglomerate, sandstone, carbonaceous shale, and mudstone.||||||
27850|Muncon Volcanics|22977|5|Briefly described|p67 Fig.2|Triassic|Triassic|||||||
27850|Muncon Volcanics|23037|6|Mentioned|p116||Triassic|||||||
27850|Muncon Volcanics|23468|5|Briefly described|Fig 4 p 298|||||||||
27850|Muncon Volcanics|24491|4|Described|p23|Triassic|Triassic|Small outlier of this unit overlies Galloway Plains Tonalite on Mount Redshirt.||||||
27850|Muncon Volcanics|24615|5|Briefly described|CD|Triassic|Triassic|[Rvm].  Basalt to andesite, volcaniclastic pebble conglomerate, sandstone, siltstone, volcanic breccia, tuff.||||||
27850|Muncon Volcanics|30059|6|Mentioned|p5|||Triassic age.||||||
27850|Muncon Volcanics|30451|3|Fully described|p67|||Lower or Middle Traissic age.||||||24-SEP-08
27850|Muncon Volcanics|30474|6|Mentioned|p252|||Refers Cameron (1972)||||||
27850|Muncon Volcanics|30655|3|Fully described|p17|||See also Table 1.||||||24-SEP-08
27850|Muncon Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
27850|Muncon Volcanics|31117|6|Mentioned|p378|||||||||
27850|Muncon Volcanics|31659|6|Mentioned|p73|||Of McKellar (1967) - MONTO sheet.||||||09-JUN-09
27850|Muncon Volcanics|33774|3|Fully described|p40|||||||||
27850|Muncon Volcanics|34408|6|Mentioned|p185|||On Table||||||
27850|Muncon Volcanics|35937|6|Mentioned|Fig.4|||||||||
27850|Muncon Volcanics|36235|6|Mentioned|p181|||See also Fig.1.||||||
27850|Muncon Volcanics|36333|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
27850|Muncon Volcanics|36488|6|Mentioned|Plate 1|||||||||
27850|Muncon Volcanics|36825|6|Mentioned|p2|||||||||
27850|Muncon Volcanics|37109|5|Briefly described|p283|||||||||
27850|Muncon Volcanics|37119|6|Mentioned|Fig.1|||||||||
27850|Muncon Volcanics|38306|6|Mentioned|p509|||||||||
27850|Muncon Volcanics|38447|6|Mentioned|Map legend|Triassic|Triassic|||||||
27850|Muncon Volcanics|39445|5|Briefly described|Table 9|||||||||
27850|Muncon Volcanics|39505|6|Mentioned|p170|||||||||
27850|Muncon Volcanics|39632|6|Mentioned|p209|||||||||
27850|Muncon Volcanics|40479|6|Mentioned|p32|||||||||
27850|Muncon Volcanics|40623|5|Briefly described|p80|||||||||
27850|Muncon Volcanics|41246|6|Mentioned|Map legend|Triassic||||||||
27850|Muncon Volcanics|41272|6|Mentioned|M 1of1 N13|||||||||
27850|Muncon Volcanics|41738|6|Mentioned|p168|||||||||
27850|Muncon Volcanics|42370|5|Briefly described|Fig.3 P317|||||||||
27850|Muncon Volcanics|44360|4|Described|p3,20,35,36,map||Triassic|To be defined by Dear 1967.||||||
27850|Muncon Volcanics|44379|2|Defined|p2,20-25,map||Triassic|||||||
27850|Muncon Volcanics|50190|6|Mentioned|p17, 34|||||||||
27850|Muncon Volcanics|50214|5|Briefly described|Map Legend|Early Triassic|Early Triassic|||||||
27850|Muncon Volcanics|60282|5|Briefly described|p10|Triassic|Triassic|Predominantly basic lavas in the MONTO sheet area.||||||
27850|Muncon Volcanics|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Yarrol Trough.||||||17-MAR-09
27850|Muncon Volcanics|61730|6|Mentioned|p1013|||Of Bryan et al (2001) for basaltic rocks in the Dooloo Creek area; but probably now included within the Three Moon Conglomerate, Lochenbar and Mount Hoopbound Formations? (unclear in text).||||||21-APR-06
27850|Muncon Volcanics|61772|6|Mentioned|p129, p130 Fig. 5||Late Triassic|In New England Orogen.||||||24-SEP-08
27850|Muncon Volcanics|61782|6|Mentioned|p282|||||||||
27850|Muncon Volcanics|65388|4|Described|p207-208; p 204 Fig72; p209|Middle Triassic|Early Triassic|"Nobbies Basalt" by Dear (1963), the name Muncon Volcanics was established by Dear (1968) for a succession of siltstone, basic to intermediate lava, and "agglomerate" unconformably overlying Palaeozoic rocks near Mount Muncon, south of Cania in SCORIA. Unconformably overlie Rockhampton Group, Youlambie Conglomerate, Wingfield Granite. Unconformably overlain by Precipice Sandstone. Correlated with Native Cat Andesite. Age based on plant fossils.||||||
27850|Muncon Volcanics|65452|5|Briefly described|p2-4, p35-p36|Late Triassic|Middle Triassic|Southern Yarrol Province. Age based on plant fossils, stratigraphic relationships and correlation with other units. Similar geochemistry to Agnes Water Volcanics. Trace elements briefly described.|||||Interbedded volcaniclastic sediments and minor basaltic to andesitic lava in lower part. Basaltic to andesitic lava accompanied by tuffs, volcanic breccia and minor conglomerate in upper part.|05-MAR-19
27850|Muncon Volcanics|67203|5|Briefly described|p3, p5, p8|Middle Triassic|Early Triassic|Kalpowar and Bobby Range areas. Recently divided into numerous individual units including Bobby Volcanics.|||||Tuffaceous sandstone, carbonaceous shale and mudstone overlain by andesitic lava and tuff and andesitic and trachytic agglomerate.|
27850|Muncon Volcanics|68008|3|Fully described|p142-143, p191-195, p202, p209, p213-214|Middle Triassic|Early Triassic|See also p218, p233, p530, p565. Dear (1968), named after Mount Muncon, S of Cania. Previously used informally by McKellar (1967) for the basal part of a volcanic sequence NE of Monto, now mapped as unnamed Triassic volcanics. Dear et al. (1971) applied the name to almost all Triassic volcanic units in the Monto 250k sheet area: most have been allocated to separate units eg Cynthia beds (Whitaker et al., 1974) and Robert Granite. The type area is SW of Cania. Exposed beneath Precipice Sandstone escarpments. Lithologies described in some detail. Geochemistry described: similar to Native Cat Andesite. Over 150m thick. Age from plant species (listed). Rb-Sr data tabulated.||||Overlies Wingfield Granite nonconformably, and Rockhampton Group and Youlambie Conglomerate unconformably and/or faulted against. Is overlain unconformably by Precipice Sandstone.|Interbedded volcaniclastic pebble conglomerate, tuffaceous sandstone, siltstone and minor basaltic to andesitic lava; then basaltic to andesitic lavas dominate with tuffs, volcanic breccia and minor pebble conglomerate. Thin trachyte flows near top.|
27850|Muncon Volcanics|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Toogoolawah Group and Native Cat Andesite, are all mapped under the symbol, Rvm.||||||
27850|Muncon Volcanics|68679|5|Briefly described|p312-313,p338,p398,p434,p441, p444, p471|Middle Triassic|Early Triassic|Dear et al. (1971). Agnes Water-Biloela region, northern New England Orogen. Most volcanics in this area were included in this unit before detailed division (Murray et al., 2012). The only remaining component is thin volcaniclastics and mafic to intermediate volcanics near Cania Dam. Continental arc during Hunter-Bowen Orogeny. Age range from plant fossils.||||Correlated with Native Cat Andesite.|Basal interbedded carbonaceous siltstones, volcaniclastic sandstones and pebbly conglomerates with minor basaltic to andesitic lavas; upper parts are mainly basaltic to andesitic lava flows, tuffs, volcanic breccia and minor pebble conglomerate.|
27850|Muncon Volcanics|73450|6|Mentioned|p11, p20|||Previously mapped to include Molangul Granite (Ellis, 1974).||||||
22473|Munderra Granodiorite|23423|5|Briefly described|p314 Table 7.4|Early Permian|Late Carboniferous|Of the Claret Creek Supersuite.||||||01-JUN-09
22473|Munderra Granodiorite|23502|5|Briefly described|Map Legend||Late Carboniferous|Of Claret Creek Ring Complex, Claret Creek Supersuite.||||||01-JUN-09
22473|Munderra Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 362. I-Type.||||||
22473|Munderra Granodiorite|23616|6|Mentioned|Table 3 p55|||||||||
22473|Munderra Granodiorite|23624|4|Described|p25|Late Carboniferous|Late Carboniferous|Of the Claret Creek Supersuite.||||||01-JUN-09
22473|Munderra Granodiorite|43259|4|Described|Appendix 1,p41.||Late Carboniferous|Rb-Sr age is 301 Ma.||||||
22473|Munderra Granodiorite|60425|4|Described|p51 Tb. 3, p282-3 Appdx. |Early Permian|Early Permian|Of Claret Creek Suite (Claret Creek Sup'ste);also part of Claret Creek Ring Complex.Cuts into Claret Creek Volcs.Age: >/-290Ma (Rb-Sr). Med.-gr.,even-gr.to locally porph. biotite-hornblende granodiorite+ tonalite; minor leucocratic granodiorite. I-type.||||||07-FEB-11
22473|Munderra Granodiorite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Medium-grained, even-grained to (locally) porphyritic biotite-hornblende granodiorite and tonalite; minor leucocratic granodiorite.|
22473|Munderra Granodiorite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Medium-grained, even-grained to (locally) porphyritic biotite-hornblende granodiorite and tonalite; minor leucocratic granodiorite.|
22473|Munderra Granodiorite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.|Claret Creek Supersuite.||||
36389|Mundic Suite|23422|5|Briefly described|p184, p219 table 6.12|Late Permian|Early Permian|Of Woodstock Supersuite.||||||
36389|Mundic Suite|23431|5|Briefly described|p537|||Kennedy Province.||||||
36389|Mundic Suite|69593|5|Briefly described|p494|Permian|Permian|Also includes unnamed dykes and plugs.|~285-265 Ma (Rienks, 1997).|Woodstock Supersuite.|Mundic Igneous Complex.||Biotite and hornblende-biotite granite and granodiorite; minor diorite/gabbro, andesite and rhyolite.|
78944|Mungunal Granite|65388|2|Defined|p268-269, p262, p256, 273, 331|Late Carboniferous|Late Carboniferous|May post-date Glen View Quartz Monzodiorite. Intrudes Rockdale Granite. Interpreted to pre-date Ravenscraig Gabbro. Age: K-Ar biotite age of 307+/-6Ma (Webb & McDougall, 1968). Pale pinkish brown to pale pink, medium-grained, uneven-grained to slightly porphyritic (in K-feldspar), leucocratic biotite monzogranite.||||||
78944|Mungunal Granite|68679|5|Briefly described|p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.|307 +/- 6 Ma (K-Ar: Webb and McDougall, 1968).|||Intrudes Rockdale Granite.|Pale pinkish brown to pale pink, medium-grained, uneven grained to slightly porphyritic (alkali feldspar), leucocratic biotite monzogranite.|
38875|Munholme Quartz Diorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
38875|Munholme Quartz Diorite|24488|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38875|Munholme Quartz Diorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgmu].  Grey medium-grained biotite-hornblende quartz diorite and tonalite, biotite-augite-hornblende diorite.||||||
38875|Munholme Quartz Diorite|68008|2|Defined|p334, p338, p411-413, p637|||New unit: not shown in Dear et al. (1971). A small (2.5 x 1.5 km) intrusion on the W side of Munholme Creek (after which it is named), 40km N of Monto. The type area is along an unnamed NE-flowing tributary of Munholme Creek in the northern part of the outcrop. Forms low, locally steep ridges. Geophysics briefly described and modelled. Geochemistry described. Not dated; age from most plutons in the region. The Rockhampton Group forms some roof pendants. Hosts a variety of mineralisation styles including the Silver Star deposit and the Nestor (gold) prospect.||||Intrudes Three Moon Conglomerate and Rockhampton Group.|Dominant rock type is grey, medium-grained biotite-hornblende quartz diorite to tonalite; subsidiary biotite-augite-hornblende diorite.|
38875|Munholme Quartz Diorite|68679|6|Mentioned|p427|||Geochemistry briefly described.||||||
23852|Muntalunga Range Granite|23509|5|Briefly described|Map Legend||Permian|||||||
23852|Muntalunga Range Granite|40607|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
23852|Muntalunga Range Granite|40954|6|Mentioned|p133|||||||||
26066|Muralug Ignimbrite|23421|4|Described|Table 5.3 p164.||Late Carboniferous|of Torres Strait Volcanic Group. Thickness: +150m. Intruded by Badu Suite.||||||
26066|Muralug Ignimbrite|32564|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
26066|Muralug Ignimbrite|33880|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26066|Muralug Ignimbrite|33883|6|Mentioned|p9|||||||||
26066|Muralug Ignimbrite|34582|2|Defined|p530|Permian|Carboniferous|Carboniferous - Permian. See also P533, Table 1||||||
26066|Muralug Ignimbrite|45076|4|Described|p37|||Carb.?  See also P102.||||||
26066|Muralug Ignimbrite|72983|6|Mentioned|p61|||||Torres Strait Volcanic Group||||
29598|Murdering Creek Metamorphics|22845|2|Defined|p7,15-18,30,33,54|Early Carboniferous|Late Devonian|Correlates to Anderson Creek Phyllite and Talamy Schist.||||||
29598|Murdering Creek Metamorphics|22846|6|Mentioned|p58,68,9||Devonian|Intruded by Station Creek Quartz Monzonite and Black Snake Porphry.||||||
29598|Murdering Creek Metamorphics|23799|5|Briefly described|p21|||Geological Province: D'Aguilar Subprovince.||||||
29598|Murdering Creek Metamorphics|43588|6|Mentioned|p30||Late Devonian|||||||
29598|Murdering Creek Metamorphics|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
30205|Murronga Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Parent: McBride Basalt Group. Age: 0.15Ma. Geological Province: Georgetown Region.||||||08-JUL-15
30205|Murronga Basalt|23619|4|Described|p28 table 1||Pleistocene|Olivine basalt. Of the McBride Basalt Group in the McBride Basalt Province.||||||
30205|Murronga Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
30205|Murronga Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
30205|Murronga Basalt|50202|5|Briefly described|Map legend|Quaternary|Quaternary|Of the McBride Basalt Group. Olivine basalt. Age 0.15Ma.||||||30-APR-15
30205|Murronga Basalt|68344|5|Briefly described|Map legend.|Quaternary|Quaternary||0.15 Ma.|Unit in McBride Basalt Group.|||Olivine basalt.|
30205|Murronga Basalt|68576|5|Briefly described|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30205|Murronga Basalt|73115|6|Mentioned|p: 28-29, 39, 43, 48, 53, 59, 63, 65|Pleistocene|Pleistocene|McBride Basalt Province. Associated with persistent wet areas / springs.|0.15-0.2 Ma|||||
78313|Myally Supersequence|63866|5|Briefly described|p53, p58, p60-p61|Statherian|Statherian|Leichhardt Superbasin.|c. 1780-1760 Ma||Includes the Eastern Creek Volcanics, Lena Quartzite, Whitworth Quartzite, Alsace Quartzite and the Bortala Formation.|Apparently coeval witbh the Argylla Formation.||
78313|Myally Supersequence|65505|5|Briefly described|979, 981|Proterozoic|Proterozoic|Age: 1780-1765 Ma. Overlies the Guide Supersequence. Includes Eastern Creek Volcanics, Lena Quartzite, Myally Subgroup.||||||
78313|Myally Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||Leichhardt Superbasin.|~1775-1760 Ma.|||Overlies Guide Supersequence. Is overlain by Quilalar Supersequence.||
78313|Myally Supersequence|68021|5|Briefly described|p134 Fig 3, p135, 136|Statherian|Statherian|Leichhardt Superbasin. Fluviatile to lacustrine sedimentary packages. Age equivalent to Marraba Volcanics?|~1780-~1765 Ma||Includes Myally Subgroup, Eastern Creek Volcanics, and Lochness Formation, towards the top.|Lower part equivalent to Argylla Formation.||
78313|Myally Supersequence|68575|6|Mentioned|p40|||||||||
78313|Myally Supersequence|68732|5|Briefly described|p159, p161, p165-166, p169-171|||Interbedded with the Eastern Creek Volcanics. Includes the Lochness Formation, Whitworth Quartzite, Bortala Formation, Alsace Quartzite, Lena Quartzite, Argylla Formation, Timberoo Member, Mount Start Member, Cone Creek Volcanic Member. Age of maximum flooding surface; from Bortala Formation.|1773 +/- 2 Ma.||||Comprises siliciclastic sedimentary rocks.|01-DEC-17
78313|Myally Supersequence|69591|6|Mentioned|p27, p32-33|||Leichhardt River Domain, Leichhardt Superbasin, Mount Isa Province. Represents the second stage of crustal extension. Includes Eastern Creek Volcanics and Myally Subgroup.||||||
78313|Myally Supersequence|72912|5|Briefly described|p12.|Statherian|Statherian|Of Leichhardt Superbasin.||||||
78313|Myally Supersequence|72919|6|Mentioned|p63|||Deposition occurred between ca. 1780 Ma and ca. 1765 Ma (Neumann et al., 2006).||||||
76902|Myla Granite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event||Williams Supersuite|||Coarse-grained, megacrystic mafic-rich hornblende-biotite granite|
76902|Myla Granite|69591|5|Briefly described|p59||||1520 +/- 8 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.|||Coarse-grained, megacrystic mafic-rich hornblende-biotite granite.|
76902|Myla Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Coarse-grained, megacrystic mafic-rich hornblende-biotite granite; granodiorite (mapped separately).|05-MAY-16
76902|Myla Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes an unnamed granodiorite member.||Williams Supersuite.|Includes one unnamed member.||Coarse grained, megacrystic mafic-rich hornblende-biotite granite.|
76902|Myla Granite|71592|5|Briefly described|Appendix A.|||Soldiers Cap Domain, Mount Isa Orogen.|1520+/-8 Ma (U-Pb zircon SHRIMP)||||Granite.|
22494|Myola Granite|23049|3|Fully described|p26|Early Devonian|Late Silurian|Age: 398+/-12Ma. of Amarra Suite.||||||
22494|Myola Granite|23283|2|Defined|p21|Devonian|Silurian|||||||
22494|Myola Granite|23422|5|Briefly described|p177, p216 Table 6.10|Middle Devonian|Early Devonian|Of Amarra Supersuite.||||||
22494|Myola Granite|23505|5|Briefly described|Map legend|Devonian|Silurian|of Amarra Supersuite.||||||
22494|Myola Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
22494|Myola Granite|69592|5|Briefly described|p292-293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~6 km2. Forms low hills.|398 +/- 12 Ma (K-Ar; Webb, 1971).|Amarra Suite.|||Cream to pink, medium-grained, biotite-muscovite granite comprises strained quartz, mainly interstitial microcline and orthoclase, subhedral altered plagioclase, muscovite, minor biotite and opaques.|
81119|Myrrlumbing Basalt|69599|5|Briefly described|p594|Pliocene|Pliocene||3.48 Ma.|||Is overlain by the Campaspe Formation.||
81119|Myrrlumbing Basalt|73115|6|Mentioned|p: 76-77, 90, 94, 99, 105, 110, 115, 120|Pliocene|Pliocene|Nulla Basalt Province.|3.48 Ma|||Interfingers with Campaspe Formation.||
25318|Myrtlevale Formation|22800|6|Mentioned|p585||Famennian|||||||
25318|Myrtlevale Formation|23422|5|Briefly described|p180, p205 Table 6.3|Early Carboniferous|Late Devonian|Of Keelbottom Group.||||||
25318|Myrtlevale Formation|23424|6|Mentioned|p346|||Burdekin Basin Province.||||||
25318|Myrtlevale Formation|23430|5|Briefly described|p506||Devonian|Also see Plate 14.11. Of Keelbottom Group. Burdekin Basin Province.||||||
25318|Myrtlevale Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Keelbottom Group.||||||14-NOV-07
25318|Myrtlevale Formation|23522|5|Briefly described|p250 Fig 6|Famennian|Famennian|Of Keelbottom Group.||||||
25318|Myrtlevale Formation|23893|5|Briefly described|p16|Early Carboniferous|Late Devonian|Of Keelbottom Group.  Geological Province: Burdekin Basin.||||||
25318|Myrtlevale Formation|24577|4|Described|p752 Fig. 1, p755 Fig. 2|Famennian|Famennian|Of the Dotswood Group. Overlies the Julia Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
25318|Myrtlevale Formation|24610|5|Briefly described|p62|Famennian|Famennian|Of the Keelbottom Group. Geological Province: Burdekin Basin. Contains Famennian Brachiopods.||||||14-NOV-07
25318|Myrtlevale Formation|24612|5|Briefly described|p7|Late Devonian|Late Devonian|Of the Keelbottom Group. Geological Province: Burdekin Basin.||||||
25318|Myrtlevale Formation|24613|2|Defined|p9 Fig. 4, p63-64|Famennian|Famennian|Of Keelbottom Group. Unconformable on Dotswood Group; conformable on Julia Fm; conformable below Lollypop Fm. Max. thickness: 460m. Geological province: Burdekin Basin. Detailed lith incl.||||||07-FEB-11
25318|Myrtlevale Formation|24614|4|Described|p190, p195|Famennian|Famennian|Basal unit of the Keelbottom Group. Max. thickness: ~460m; 340m in type section. Geological Province: Burdekin Basin. See also p191 Fig. 1, p193 Fig. 2.||||||07-FEB-11
25318|Myrtlevale Formation|37573|4|Described|p216|||See also Fig.13||||||
25318|Myrtlevale Formation|39686|6|Mentioned|p72|||||||||
25318|Myrtlevale Formation|39735|6|Mentioned|p18|||||||||
25318|Myrtlevale Formation|42547|6|Mentioned|p66|||||||||
25318|Myrtlevale Formation|42689|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25318|Myrtlevale Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
25318|Myrtlevale Formation|42933|5|Briefly described|Fig.94 p258|||||||||
25318|Myrtlevale Formation|43095|5|Briefly described|Plate 2|||of Keelbottom Group||||||
25318|Myrtlevale Formation|43213|5|Briefly described|p74|||Burdekin Basin. Contains conodonts from the marginifera Zone: is thus younger than the Greybank Volcanics.||||Correlated with Mount Wyatt Formation (Drummond Basin).||
25318|Myrtlevale Formation|43933|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Of Keelbottom Group.||||||
25318|Myrtlevale Formation|45097|6|Mentioned|p22|||Famennian. Correlation chart||||||
25318|Myrtlevale Formation|62522|5|Briefly described|p21|||of Keelbottom Group. Clean, calcareous sandstones, in places fossiliferous. Unconformably to disconformably overlies Dotswood Group (that is over Julia Formation).||||||14-NOV-07
25318|Myrtlevale Formation|64783|6|Mentioned|p102|Famennian|Famennian|Marine transgression in Burdekin Basin.||||||15-NOV-17
25318|Myrtlevale Formation|65214|6|Mentioned|p281, p283|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
25318|Myrtlevale Formation|67402|4|Described|p239, p246, p247, p248|Famennian|Famennian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under mainly shoreline to shelfal marine environments. ||||Overlain by the Lollypop Formation.|Sandstone, siltstone and mudstone.|
25318|Myrtlevale Formation|68297|5|Briefly described|p186, 194|Late Devonian|Late Devonian|Burdekin-Star Basin/shelf. Include Late Devonian vertebrate fossil assemblages and Famennian conodonts from ~mid formation.||||||
25318|Myrtlevale Formation|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Julia Formation. Is overlain conformably by Lollypop Formation.|Green to grey, fossiliferous mudstone, fine- to medium-grained feldspathic to lithic sandstone and minor sandy limestone; marine and plant fossils.|
25318|Myrtlevale Formation|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Julia Formation. Is overlain conformably by Lollypop Formation.|Green to grey, fossiliferous mudstone, fine- to medium-grained feldspathic to lithic sandstone and minor sandy limestone; marine and plant fossils.|
25318|Myrtlevale Formation|68419|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.||Of the Keelbottom Group.||Conformably overlain by the Lollypop Formation. Conformably underlain by the Julia Formation, Dotswood Group.|Green to grey, fossiliferous mudstone, fine to medium-grained feldspathic to lithic sandstone and minor sandy limestone; marine and plant fossils.|
25318|Myrtlevale Formation|68420|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin. But map symbol (Dkm) implies unit is entirely Devonian.||Of the Keelbottom Group.||Conformably overlain by the Lollypop Formation. Conformably underlain by the Julia Formation, Dotswood Group.|Green to grey, fossiliferous mudstone, fine to medium-grained feldspathic to lithic sandstone and minor sandy limestone; marine and plant fossils.|27-AUG-14
25318|Myrtlevale Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4, p187|Upper Devonian|Upper Devonian|Burdekin Basin. Basal transgressive formation. < 460 m thick. Siliciclastic shoreline to inner shelf facies. Diverse benthic fauna mainly of brachiopods but including bivalves, gastropods, and crinoids.||Of the Keelbottom Group.|||Comprises locally conglomeratic basal pebbly quartz sandstone; fine- to coarse-grained feldspathic calcareous sandstone, micaceous siltstone and mudstone. Common shelly beds and local coquina.|
25318|Myrtlevale Formation|70740|5|Briefly described|p49|Famennian|Famennian|Burdekin Basin. Hosts a species of Chonetes sp., fossils that are also found in the Mount Wyatt Formation. ||||Equivalent to the Mount Wyatt Formation.||
24415|Myubee Igneous Complex|24197|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite? Geological Province: Mount Isa Inlier.||||||07-FEB-11
24415|Myubee Igneous Complex|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24415|Myubee Igneous Complex|37862|4|Described|p585|||||||||
24415|Myubee Igneous Complex|38310|6|Mentioned|p237|||||||||
24415|Myubee Igneous Complex|38350|4|Described|p19|||||||||
24415|Myubee Igneous Complex|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24415|Myubee Igneous Complex|39445|6|Mentioned|p43|||See also Table 2||||||
24415|Myubee Igneous Complex|39622|6|Mentioned|p27|||||||||
24415|Myubee Igneous Complex|40840|6|Mentioned|Map legend|||||||||
24415|Myubee Igneous Complex|45161|4|Described|p32|||||||||
24415|Myubee Igneous Complex|45166|5|Briefly described|p34|||||||||
24415|Myubee Igneous Complex|46976|6|Mentioned|Fig.1|||||||||
24415|Myubee Igneous Complex|49009|2|Defined|p30|Proterozoic|Proterozoic|Mapped as Wonga Granite by Carter & Opik (1963).||||||
24415|Myubee Igneous Complex|49041|5|Briefly described|Table 2|||||||||
24415|Myubee Igneous Complex|50100|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Burstall Suite (Wonga Batholith).  Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||
24415|Myubee Igneous Complex|50536|5|Briefly described|p1.1, 6.2|||Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||
24415|Myubee Igneous Complex|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Gabbro, leucocratic granite.||||||
24415|Myubee Igneous Complex|65396|6|Mentioned|p319|||Mount Isa Inlier.|c.1740 Ma.|||||
24415|Myubee Igneous Complex|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event. Informally subdidvided in to 2 units - g and o.||Wonga Suite, Burstall Suite|||Medium-grained foliated granite. Medium to coarse-grained gabbro; minor diorite and amphibolite|
24415|Myubee Igneous Complex|72596|6|Mentioned|p40, 46|Statherian|Statherian|Correlated with / compositionally similar to the granitic component of the Mount Erle Complex, and the Overlander, Revenue and Burstall granites (see Bultitude et al., 1982; Blake et al., 1984). Geochronologic constraint given as C. Lewis & S. Jones, GA, written communication, August, 2019.|ca. 1726 Ma|Burstall Suite||||
24415|Myubee Igneous Complex|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Medium-grained foliated granite and Medium to coarse-grained gabbro; minor diorite and am phibolite.|
24415|Myubee Igneous Complex|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Wonga Suite||Shown as equivalent age to other Wonga Suite units and Burstall Suite units.|Medium-grained foliated granite. Medium to coarse-grained gabbro; minor diorite and amphibolite.|
24415|Myubee Igneous Complex|72799|4|Described|p1, p3, p5, p18-24|||New slightly younger SHRIMP U-Pb age of 1727 +/- 5 Ma is a minimum age for igneous crystallisation of the granite because there is evidence of post-crystallisation isotopic disturbance. Passchier (1992) suggested this unit is slightly younger than the nearby Revenue Granite, based on structural criteria. Roughly circular (ca 2.5 km2); crops out ca 16 km north of Duchess. Consists of an outer zone of granite and metadolerite surrounding a core of layered gabbro.||||Intrudes Corella Formation. Coeval with Revenue Granite[?], Mount Erle Igneous Complex, and Burstall Granite.|Includes granite, metadolerite, and layered gabbro. Granite contains angular inclusions of coarse-grained gabbro up to several metres across.|
24415|Myubee Igneous Complex|73529|5|Briefly described|p11|||Consists of two circular-shaped intrusions, the 900 m wide Myubee Gabbro surrounded by the ~1600 m wide Myubee Granite. Intruded by small volumes of syenite and pegmatite. See also Myubee Igneous complex p8, p10-11.|||Myubee Gabbro, Myubee Granite|Intruded Corella Formation||
24415|Myubee Igneous Complex|73553|4|Described|p2-3, p8, p43, p59, p146, p153,|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Roughly circular. Tentatively included in the Burstall Suite by Budd et al., (2001). Granitic rocks show mainly red tones on radiometric images and low magnetic responses, white tones and moderately high to high responses in NW part. Mafic core shows dark tones on radiometric images and low (southern and central parts) to high (northern) magnetic responses. Cut by a northerly trending dolerite dyke. Misspelt Mubee Igneous Complex p163. See also p158, p165-167, p169-p171, p173, p175-p178, p221, p224, p228, p266.|1727+/-5 Ma SHRIMP U-Pb, 1718+/-14 Ma U-Pb LAICPMS|Burstall Suite||Intrudes Corella Formation, intruded by Lakeview Dolerite|Comprises a core of layered gabbro surrounded by granitic rocks. Includes olivine-rich gabbro or norite, pyroxene gabbro, hornblende-pyroxene gabbro, (clinopyroxene-) hornblende gabbro, hornblende leucogabbro/diorite/monzodiorite, syenite.|03-FEB-23
24416|Mywyn Granite|23291|5|Briefly described|p88 Tb. 3.7|||Parent: unassigned, possibly Forsayth Supersuite. Age: probably Mesoproterozoic. Geological Province: Georgetown Region.||||||08-JUL-15
24416|Mywyn Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 827. S-Type.||||||
24416|Mywyn Granite|23619|4|Described|p42 Table 2||Proterozoic|Intrudes Einasleigh Metamorphics. Also see p6. Georgetown Province.||||||
24416|Mywyn Granite|24197|5|Briefly described|p17, p79 tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
24416|Mywyn Granite|39981|2|Defined|p102|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||11-MAY-15
24416|Mywyn Granite|40542|6|Mentioned|p98|||||||||
24416|Mywyn Granite|41680|3|Fully described|p117|||||||||
24416|Mywyn Granite|43113|4|Described|Table 2 p27|||Middle Proterozoic age.||||||
24416|Mywyn Granite|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age.||||||
24416|Mywyn Granite|43259|4|Described|Appendix 1,p54.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
24416|Mywyn Granite|50201|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
24416|Mywyn Granite|50202|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Grey, foliated, porphyritic biotite granite with K-feldspar megacrysts to 3cm.||||||
24416|Mywyn Granite|50537|5|Briefly described|p1.2, 1.4, 2.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.||||||
24416|Mywyn Granite|63866|6|Mentioned|p77|||||Forsayth Supersuite||||
24416|Mywyn Granite|66529|5|Briefly described|p60, p63  |Proterozoic|Proterozoic|Hosts the Oasis U prospect.|c.1558 Ma (Kositcin, unpublished data).||||Foliated, feldspar porphyritic biotite granite.|
24416|Mywyn Granite|67341|5|Briefly described|p60-62|Calymmian|Calymmian|Etheridge Province. The Oasis uranium prospect, hosted in a shear zone which cuts this unit, was probably sourced from the granite. Magmatic crystallisation age.|1559 +/- 3 Ma (SHRIMP U-Pb zircon).|Forsayth Supersuite.|||Cream-pink, strongly foliated, feldspar-porphyritic biotite granite. S-type.|
24416|Mywyn Granite|67430|5|Briefly described|p24, 27, 31-32, 70|Mesoproterozoic|Mesoproterozoic|Etheridge Province. Hosts the Oasis U deposit, 20km NW of The Lynd, NE QLD. U occurs as a tabular deposit in a (mylonitic biotite-quartz schist) shear zone, up to 15m thick. Mineralisation is constrained to ~440 - 433 Ma.|1559 +/- 3 Ma (Neumann and Kositcin, in prep.).||||Foliated, feldspar-porphyritic biotite granite.|
24416|Mywyn Granite|68344|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Grey, foliated, porphyritic biotite granite with K-feldspar megacrysts to 3 cm.|
24416|Mywyn Granite|68346|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Grey, foliated, porphyritic biotite granite with K-feldspar megacrysts to 3 cm.|
24416|Mywyn Granite|68576|6|Mentioned|Q_11: p31-32|Mesoproterozoic|Mesoproterozoic|E of Einasleigh. Poor exposures.||||||
24416|Mywyn Granite|69591|5|Briefly described|p81, p83|Mesoproterozoic|Mesoproterozoic|Warnick (1989). SE of Einasleigh. Although not part of the Forsayth Batholith, this unit probably belongs in the Forsayth Supersuite. Has a strong radiometric signature, high in K, U and Th; hosts uranium deposits.|1559 +/- 3 Ma (Neumann and Kositcin, 2011).||||Strongly foliated, porphyritic, biotite granite.|
24416|Mywyn Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1559+/-2.9 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
24416|Mywyn Granite|73642|5|Briefly described|p4 Tb.1, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier.|1559+/-6 Ma|Forsayth Supersuite||||
38876|Nagoorin beds|24489|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
38876|Nagoorin beds|24615|5|Briefly described|CD|Tertiary|Tertiary|[Tn].  Mudstone, siltstone, oil shale, sandstone, shale, conglomerate.||||||
38876|Nagoorin beds|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||
38876|Nagoorin beds|67402|5|Briefly described|p239, p262, p263|||Nagoorin Graben. Unsuitable reservoir for the storage of carbon dioxide. Deposited in fluvial to lacustrine environments. Up to 1100m thick. |||||Carbonaceous shale, oil shale, sandstone, mudstone, siltstone, conglomerate and low grade coal.|
38876|Nagoorin beds|68008|3|Fully described|p199, p277-279, |Eocene|Eocene|Dear et al. (1971). Nagoorin Graben. All units except the base contain significant oil shale deposits: total is c.3 billion barrels. Contains significant coal and coal seam gas resources. Maximum thickness is 870m. Mid- to late- Eocene (by analogy with other oil shale sequences).||||Overlies Calliope beds, Mount Alma and Wandilla Formations. Is faulted against Bobby Volcanics, Calliope beds, Mount Alma Formation, Rockhampton Group and Littlemore Granodiorite.|Sandstone with minor conglomerate and lignitic oil shale at the base, overlain by a thick sequence of carbonaceous oil shale with intervals of green mudstone, siltstone and fine-grained sandstone. Some rock types contain abundant carbonate.|
38876|Nagoorin beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
38876|Nagoorin beds|68679|6|Mentioned|p312-313|Paleogene|Paleogene|Northern New England Orogen.||||||
38876|Nagoorin beds|69599|5|Briefly described|p586-588|Eocene|Eocene|Dear et al. (1971); Swarbrick (1974). Nagoorin Graben. 720m thick (including intrusives) in Boyne River 2C well. Lacustrine and fluvial deposits during syn-depositional faulting. Appears as Nangorin beds on p586. RELATED UNITS (continued): Also correlated (at least partly) with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; Flinders Dolomite; see COMMENTS for more.|Interbedded oil shale, carbonaceous shale, coal, siltstone, mudstone, claystone with subordinate conglomerate, sandstone and very minor calcareous siltstone and limestone. Intruded by dolerites and basalts.|
38876|Nagoorin beds|72297|5|Briefly described|p754-755|Eocene|Eocene|Nagoorin Graben, 70km SW of Gladstone. Hosts the Nagoorin and Nagoorin South oil shale deposits. Described, and estimated resources tabulated.|||||Conformably interbedded cannel coal, oil shale, mudstone, siltstone, sandstone, conglomerate and minor limestone.|
27516|Namarrong Volcanic Subgroup|23291|4|Described|p40, p95 Tb. 3.10|Permian|Carboniferous|Parent: Newcastle Range Volcanic Group. Geological Province: Georgetown Region.||||||28-MAY-15
27516|Namarrong Volcanic Subgroup|23430|6|Mentioned|p493|||Kennedy Province||||||
27516|Namarrong Volcanic Subgroup|23510|5|Briefly described|Map Legend||Early Permian|of Newcastle Range Volcanic Group.||||||
27516|Namarrong Volcanic Subgroup|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27516|Namarrong Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
27516|Namarrong Volcanic Subgroup|43716|6|Mentioned|p140|||||||||
27516|Namarrong Volcanic Subgroup|43740|5|Briefly described|p10|||||||||
27516|Namarrong Volcanic Subgroup|68576|5|Briefly described|Q_11: p21|Carboniferous|Carboniferous|Forms the Namarrong Cauldron.||Newcastle Range Volcanic Group.||||
27516|Namarrong Volcanic Subgroup|69593|5|Briefly described|p485, p489-490|Permian|Permian|Tate and Kidston Subprovinces, Kennedy Igneous Association.||Newcastle Range Volcanic Group.|||A-type. Broad compositional range, from dacite/granodiorite and andesite to granite and rhyolite. Intrusives are much more abundant than eruptives.|
27516|Namarrong Volcanic Subgroup|70207|5|Briefly described|p4, p14, p81-82|Permian|Carboniferous|Previous age determinations discussed.|c.290 Ma.|Newcastle Range Volcanic Group.|Brodies Gap Rhyolite.||Includes A-type rhyolite and augite andesite.|
23859|Namul Dacite|23291|4|Described|p42,p91 Tb. 3.9|Late Carboniferous|Late Carboniferous|Included in the Cumberland Range Volcanic Group for ease of description. Thickness: 100m. Geological Province: Georgetown Region.||||||19-MAY-15
23859|Namul Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V11. Assumed to be I-Type.||||||
23859|Namul Dacite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23859|Namul Dacite|40542|6|Mentioned|p97|||||||||
23859|Namul Dacite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Cumberland Range Volcanic Group.||||||
23859|Namul Dacite|43740|4|Described|p21|||||||||
23859|Namul Dacite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of the Cumberland Range Volcanic Group. Overlies: Scrubby Creek Rhyolite.||||||01-JUL-04
23859|Namul Dacite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron.||Unit in Cumberland Range Volcanic Group.||Conformably overlies Scrubby Creek Rhyolite.|Greyish-green moderately crystal-rich, locally strongly eutaxitic, dacitic to rhyolitic ignimbrite with abundant dark metasedimentary lithic clasts.|
81100|Namur Sandstone, upper|69594|5|Briefly described|p527|Berriasian|Tithonian|Previously the Namur Sandstone Member (Gray et al., 2002), which referred to a division of the Hooray Sandstone in QLD, where it is now known as the upper Namur Sandstone. Braided fluvial deposits. Thickness from <30m to >90m.||||Overlies Westbourne Formation conformably to unconformably. Is overlain conformably by Murta Formation. Passes laterally into lower Hooray Sandstone, and Namur Sandstone (as defined in SA).|Quartzose sandstone with subordinate interbedded siltstone.|
27295|Nancy Lee Sandstone Member|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Parrot Camp Rhyolite (Croydon Volcanic Group).  Quartzofeldspathic sandstone.||||||
27295|Nancy Lee Sandstone Member|23291|5|Briefly described|p27|||Geological Province: Georgetown Region.||||||08-JUL-15
27295|Nancy Lee Sandstone Member|40218|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||21-APR-15
27295|Nancy Lee Sandstone Member|40659|2|Defined|p252|Mesoproterozoic|Mesoproterozoic|Of Parrot Camp Rhyolite.||||||21-JUN-04
27295|Nancy Lee Sandstone Member|40954|6|Mentioned|p132|||||||||
27295|Nancy Lee Sandstone Member|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
27295|Nancy Lee Sandstone Member|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Carron Rhyolite.|||Yellow-brown to purple, thin-bedded, medium to coarse quartzofeldspathic sandstone, pink-buff banded fine micaceous quartzofeldspathic sandstone, minor laminated siltstone and silicified sandstone.|
27295|Nancy Lee Sandstone Member|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Carron Rhyolite.|||Yellow-brown to purple, thin-bedded, medium to coarse quartzofeldspathic sandstone, pink-buff banded fine micaceous quartzofeldspathic sandstone, minor laminated siltstone and silicified sandstone.|
70401|Nangandie Granite|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Equigranular granite to granodiorite; red, strongly altered syenogranite.|
70401|Nangandie Granite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Granite to granodiorite; red, strongly altered syenogranite.|
23861|Nangee Granite|23430|5|Briefly described|p475||Permian|Hodgkinson Province.||||||
23861|Nangee Granite|42304|2|Defined|p18|Permian|Carboniferous|Reserved April 1988 by R.J. Bultitude||||||
23861|Nangee Granite|43083|5|Briefly described|p130-131, p258|||Of Whypalla Supersuite. Formely mapped as part of Cannibal Creek Granite. S-type. Lithology included.||||||17-JUN-09
23861|Nangee Granite|43625|5|Briefly described|p52,124,Appendix 6|||||||||
23861|Nangee Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province||||||
23861|Nangee Granite|60357|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province. Muscovite-biotite granite.||||||
23861|Nangee Granite|60425|4|Described|p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla Supersuite). Grey, fine to medium-grained, even-grained biotite-muscovite granite; extensively deformed. S-type.||||||07-FEB-11
23861|Nangee Granite|66852|5|Briefly described|p937.|||Shows evidence of syntectonic emplacement. A small (c.2 km2) pluton, truncated to its south by a WNW-ESE fault.||Unit in Whypalla Supersuite.||||
23861|Nangee Granite|69592|5|Briefly described|p248|Permian|Permian|Intrudes the Fiery Creek Slate Belt.||||Intrudes Hodgkinson Formation.||
23861|Nangee Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Curraghmore Suite.||||
80240|Nangram Seam|68117|5|Briefly described|p347, p350-352, p354|Middle Jurassic|Middle Jurassic|Surat Basin. Inertinite composition <3%. Coal analysis.||Juandah Coal Measures (lower).|||Numerous thin coal plies, mostly less than 2m thick, interspersed with mudstone, carbonaceous mudstone, siltstone, and very fine- to fine-grained sandstone. The gross seam interval is up to 40m thick.|
80240|Nangram Seam|71282|5|Briefly described|p456, p457 Fig.1, p461, p466 Fig.13|||This, and the other eight named coal seams in the Walloon Subgroup, are presented as "coal-seam groups" with the authors making the totally unjustified claim they were "following the nomenclature of Scott et al. (2007)". [The term does not appear anywhere in the 2007 article.]||Juandah Coal Measures.||||
80240|Nangram Seam|72297|5|Briefly described|p699 Fig.10.11|Jurassic|Jurassic|Surat Basin.||Juandah Coal Measures.||||
26798|Nanyeta Volcanics|23423|4|Described|p309 Table 7.3||Late Carboniferous|I-type rocks. Also see p237. Underlying unit Chillagoe Formation and Hodgkinson Formation (unconformable). Kennedy Igneous Province.||||||
26798|Nanyeta Volcanics|23446|6|Mentioned|p448 Fig.1|||||||||
26798|Nanyeta Volcanics|23503|5|Briefly described|Map Legend||Late Carboniferous|Age: ~289 +/- 10Ma.||||||
26798|Nanyeta Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V85. I-Type.||||||
26798|Nanyeta Volcanics|23616|5|Briefly described|Table 3 p55||Late Carboniferous|Unconformable on Chillagoe & Hodgkinson Formations; intruded by Late Carboniferous granites. Hodgkinson Province. Max thick: >150 m.||||||30-AUG-04
26798|Nanyeta Volcanics|29815|6|Mentioned|p994|||||||||
26798|Nanyeta Volcanics|29820|6|Mentioned|p449|||||||||
26798|Nanyeta Volcanics|31832|6|Mentioned|Table 6|||||||||
26798|Nanyeta Volcanics|33963|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26798|Nanyeta Volcanics|37613|6|Mentioned|p253|||See also Fig.1.||||||
26798|Nanyeta Volcanics|39252|6|Mentioned|Fig.11|||||||||
26798|Nanyeta Volcanics|40743|6|Mentioned|Fig.1|||||||||
26798|Nanyeta Volcanics|43060|5|Briefly described|p75|||||||||
26798|Nanyeta Volcanics|43259|4|Described|Appendix 1,p8.||Carboniferous|||||||
26798|Nanyeta Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
26798|Nanyeta Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
26798|Nanyeta Volcanics|44296|14|Not recorded|Map Legend||Carboniferous|||||||
26798|Nanyeta Volcanics|45014|2|Defined|p45-7,50-1,110-116||Early Carboniferous|Pl.15,35,38,Tb.1. (Probably Middle Carboniferous).||||||02-JUN-09
26798|Nanyeta Volcanics|45025|4|Described|p67,anal.p73|Permian|Carboniferous|||||||
26798|Nanyeta Volcanics|45065|4|Described|Table 4|||||||||
26798|Nanyeta Volcanics|45087|5|Briefly described|p97|||See also p230-232. Chem. analyses||||||21-APR-09
26798|Nanyeta Volcanics|45113|3|Fully described|p26|||Emphasis on petrography.||||||
26798|Nanyeta Volcanics|46845|6|Mentioned|p143|||||||||
26798|Nanyeta Volcanics|46879|6|Mentioned|Fig.1|||||||||
26798|Nanyeta Volcanics|48976|4|Described|p69|||Isotopic data Table 19||||||
26798|Nanyeta Volcanics|60425|3|Fully described|p17 Tb. 1, p41, p50 Tb. 3|Early Permian|Early Permian|Unconformable on Chillagoe + Hodgkinson Fms. Age: ~289+/-10Ma. Max.thickness: >150m. Mainly cream, buff, pink, red, purple, brown, green or grey rhyolitic ignimbrite+lava; minor dacite, andesite, airfall tuff, volc.breccia, tuffaceous sed. rocks; I-type||||||07-FEB-11
26798|Nanyeta Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
26798|Nanyeta Volcanics|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Chillagoe Subprovince, Hodgkinson Province.||||||
26798|Nanyeta Volcanics|69593|6|Mentioned|p483, p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
35063|Naraku Suite|22515|4|Described|p402||Calymmian|Max Age: 1500 Ma. Includes Malakoff granite and Capsize granodiorite.||||||
35063|Naraku Suite|66529|5|Briefly described|p16, p41|||Elevated concentrations of U; possible primary U source for local sandstone-hosted systems. Mis-spelt as Naruku on p41 and p92; also appears as Naruku-Williams Granite Suite on p5; on p45 as Williams-Naruku Granites and Williams-Naruku granite suite; as Williams-Naraku suite on p53.|Between 1530 and 1500 Ma.|||||
35063|Naraku Suite|73413|6|Mentioned|p1, p3, p25|Calymmian|Calymmian|IOCG mineralization in the eastern Mount Isa Inlier is spatially associated with these intrusions.|1550-1490 Ma|||||
37962|Narpa Group|61404|5|Briefly described|Map legend|Late Cambrian|Early Cambrian|Includes: Thorntonia Limestone, Steamboat Sandstone, Chabalowe Formation and Arrinthrunga Formation. Geological Province: southern Georgina Basin.||||||11-OCT-05
37962|Narpa Group|62658|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|||||||
37962|Narpa Group|62983|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|Carbonate platform deposition. Geological Province: Georgina Basin. Written in informal format as Narpa group.||||||23-JAN-07
37962|Narpa Group|64068|2|Defined|p225 App 1, p4, p57-70, p82, p7, p ix|Late Cambrian|Middle Cambrian|New name. Includes Thorntonia, Devoncourt, Georgina, Mungerebar, Selwyn Range, Pomegranate, Currant Bush, V-Creek and Mail Change Limestones; Border Waterhole, Arthur Creek, Beetle Creek, Inca, Quita, Chabalowe, Arrinthrunga, Gowers and Age Creek Formations; O'Hara and Blazan Shales; Roaring Siltstone and Steamboat and Split Rock Sandstones.||||||18-MAR-16
37962|Narpa Group|64443|5|Briefly described|p7-9, p17-p40|||Of Georgina Basin.|||Includes Arrinthrunga Formation, Arthur Creek Formation and Thorntonia Limestone.|Correlative of Barkly Group in part.||14-MAY-14
37962|Narpa Group|65336|4|Described|Map Legend|Middle Cambrian|Middle Cambrian|Of Georgina Basin. Includes Thorntonia Limestone. Unconformably overlies Kalkarindji Volcanic Group; unconformably underlies Barkly Group.||||||
37962|Narpa Group|65337|5|Briefly described|pp63-68.|||Includes all Middle to medial Upper Cambrian units in eastern and southern Georgina Basin.|||Includes Border Waterhole Formation and Currant Bush Limestone.|||
37962|Narpa Group|65341|6|Mentioned|p5, p18.||||||Includes Chabalowe Formation.|||
37962|Narpa Group|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.|||Thorntonia Limestone; Arthur Creek, Chabalowe, Arrinthrunga Formations.|Is overlain by Tomahawk Formation.|Marine bioclastic carbonate rocks, black shale and dolostone, quartz sandstone overlain by a thick succession of peritidal, evaporitic and stromatolitic limestone and dolostone, with minor quartz sandstone, siltstone and shale.|
37962|Narpa Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|||CONSTITUENTS (continued): Currant Bush, Devoncourt, Georgina,  Mail Change, Mungerebar, Pomegranate, Selwyn Range, Thorntonia, V-Creek Limestones; Split Rock, Steamboat Sandstones.|||Includes Age Creek, Beetle Creek, Border Waterhole, Inca, Kajabbi, Mount Hendry, Quita Formations; Blazan, O'Hara Shales; Roaring Siltstone. See COMMENTS  for limestone and sandstone constituents.|||
37962|Narpa Group|67870|5|Briefly described|p43|Late Cambrian|Early Cambrian|Georgina Basin.|||Thorntonia Limestone; Arthur Creek, Arrinthrunga Formations.|||
37962|Narpa Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
37962|Narpa Group|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
37962|Narpa Group|69377|5|Briefly described|map legend|Cambrian|Cambrian||||O'Hara Shale, Pomegranate Limestone, Roaring Siltstone, Thorntonia Limestone|||
37962|Narpa Group|69443|5|Briefly described|p28:3, 5, 7, 14, 16-21, 27, 32|Middle Cambrian|Middle Cambrian|Includes all Middle and early Late Cambrian rocks in the southern and eastern Georgina Basin; correlative rocks in the central and northern parts of the Basin constitute the Barkly Group. QLD constituents include Beetle Creek, Inca, Quita, Kajabbi, Gowers, Age Creek Formations; Blazan, O'Hara Shales; Devoncourt, Georgina, Mungerebar, Selwyn Range, Pomegranate, V-Creek, Mail Change Limestones; Roaring Siltstone; Split Rock Sandstone. Is correlated with Gum Ridge Formation, Anthony Lagoon Formation, Wonarah Formation, Ranken Limestone and Camooweal Dolostone (central and western Georgina Basin), and Top Springs Limestone (northern Georgina Basin). Contains a diverse fauna, particularly of trilobites.|||In NT: Chabalowe, Arrinthrunga, Arthur Creek, Border Waterhole Formations; Thorntonia, Currant Bush Limestones; Steamboat Sandstone. See Comments for QLD constituents.|Overlies Shadow Group. Gradationally overlies Colless Volcanics. Is overlain by Cockroach Group. Lateral equivalent of Wonarah Formation, Ranken Limestone and Camooweal Dolostone.||12-JUL-16
37962|Narpa Group|69591|5|Briefly described|p29, p88-90, p92, p94|Cambrian|Cambrian|Kruse and Mohammed (2005). S and E Georgina Basin. Mainly platform carbonates.|||Thorntonia, Currant Bush, V-Creek, Mail Change, Georgina, Pomegranate, Selwyn Range Limestones; Border Waterhole, Beetle Creek, Inca, Gowers, Age Creek Formations; Split Rock Sandstone; O'Hara Shale.||Peritidal dolostones, platform limestones with interbedded black shales and dark foetid limestones with interbedded black shales.|
37962|Narpa Group|69673|6|Mentioned|p111, p114 fig 92, p116||||||Includes Chabalowe Formation, Arrinthrunga Formation|||
37962|Narpa Group|70723|5|Briefly described|p22, p24-25, p30-31|Cambrian|Cambrian|Georgina Basin. Kerogen type and biomarker compositions discussed in detail.|508-504 Ma||Thorntonia, Currant Bush, Mungerebar, Georgina Limestones; Inca, Beetle Creek, Age Creek, Arthur Creek, Quita, Chabalowe, Arrinthrunga Formations; Blazan Shale; Steamboat Sandstone.|||
37962|Narpa Group|70951|6|Mentioned|p1069|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin. Includes key middle Cambrian petroleum source rocks.|||Includes Thorntonia Limestone and Arthur Creek Formation, Chabalowe Formation.|||
37962|Narpa Group|72321|5|Briefly described|Fig 2, p3|Furongian|Series 2|Elkedra Shelf/Dulcie Syncline, Toko Syncline, Burke River Structural Belt, Undilla Sub-basin, Georgina Basin. |||See Fig 2.|||
37962|Narpa Group|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Thorntonia Limestone, Border Waterhole Formation.|||
37962|Narpa Group|72415|4|Described|mapsheet|Early Ordovician|Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Thorntonia Limestone, Border Waterhole Formation.|||
37962|Narpa Group|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Arrinthrunga Formation, Steamboat Sandstone, Arthur Creek Formation and the Thorntonia Limestone.|Disconformably overlain by the Cockroach Group. Disconformably overlies the Shadow Group.||
37962|Narpa Group|72516|5|Briefly described|p11-12, p21, p85, p91-94, 135, 171, 176|Furongian|Furongian|Georgina Basin.|ca 825 Ma (max dep age)||Includes the Arrinthrunga Formation, Steamboat Sandstone, Arthur Creek Formation and Thorntonia Limestone.|||21-APR-22
37962|Narpa Group|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|||||||
37962|Narpa Group|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.|||Includes O'Hara Shale, Devoncourt Limestone, Selwyn Limestone, Roaring Siltstone, Thorntonia Limestone, Shadow Group.|Overlies Shadow Group.|Siltstone; minor chert and sandstone; lateritic rubble capping. Impure limestone, calcilutite, bituminous limestone and marl and and subordinate chert with silicified shale.|
37962|Narpa Group|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).|||Includes O'Hara Shale, Selwyn Range Limestone, Devoncourt Limestone, Roaring Siltstone, Thortonia Limestone.|Shown as unconformably overlying Shadow Group.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert and chert breccia. Siltstone and sandstone and Impure limestone, calcilutite, bituminous limestone and marl. Lateritic rubble capping.|
37962|Narpa Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
37962|Narpa Group|73083|6|Mentioned|p75||||||||Includes siliciclastics.|
37962|Narpa Group|73137|6|Mentioned|p6|Cambrian|Cambrian|||||||
37962|Narpa Group|73288|5|Briefly described|p697||||||Arthur Creek, Chabalowe Formations; Thorntonia Limestone.|||
37962|Narpa Group|73418|5|Briefly described|p4 Fig.3|Furongian|Cambrian Series 2|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin. Also includes Gowers Formation, Currant Bush Limestone, V-Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Age Creek Formation.|||Hay River Formation, Ardmore Chert, Thorntonia Limestone, Beetle Creek Formation, Inca Formation, Roaring Siltstone, Devoncourt Limestone, Selwyn Range Limestone, Pomegranate Limestone||Includes limestone, shale, siltstone, sandstone, dolomite and phosphorite/shale units.|
37962|Narpa Group|73553|6|Mentioned|p7|Cambrian|Cambrian|||||||
79129|Nash Clastics Member|70913|4|Described|p7, p8 fig 3, p10, p29-p32, App 1 maps|Middle Permian|Early Permian|Gympie Province. Named for the Nash Street and Nash Gully in Gympie. Discussed as a Member of the Rammutt Formation but also abbreviated to Nash Clastics (p24, 35, 67, 87). Reference drill holes and a reference section are mentioned. Replaces the informal Upper Nash Clastics. Equated with the lower part of Dunstan¿s (1911) First Slate Group. Distribution and fossil assemblage briefly discussed. Ranges from a few metres up to 50m thick. See also p67 fig 9, p87.||Rammutt Formation||Overlies the Calton Andesite Member. Overlain by the Pengelly Siltstone Member.|Massive or thickly-bedded, medium-coarse grained, homogeneous volcaniclastic sandstone with occasional interbeds of pebbly conglomerate, minor siltstone.|19-SEP-17
30708|Natalie Granite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1758+/-8Ma.||||||15-MAR-07
30708|Natalie Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite (part of the Wonga Batholith). Intrudes the Argylla Formation. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30708|Natalie Granite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Eastern Fold Belt Province.||||||
30708|Natalie Granite|50332|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760-1720Ma. Intruded into the Kalkadoon-Ewen Province and Eastern Fod Belt Province. Geological Province: Kalkadoon-Ewen Province and Eastern Fod Belt Province.||||||07-FEB-11
30708|Natalie Granite|50536|5|Briefly described|p1.4, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.  Age: 1778-1729 +/- 15Ma (SHRIMP).||||||08-OCT-22
30708|Natalie Granite|63866|4|Described|p60|Statherian|Statherian|Wonga Belt. Numeric age is interpreted as to record inheritance, possibly from felsic volcanics of the Argylla Formation. A U-Pb TIMS date of 1742 +/- 13 from the granite at the Wonga Waterhole is within error of the other provided age.|1778 +/- 15 Ma (U-Pb zircon)|Wonga Suite||||
30708|Natalie Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier.|1729 +/- 5 Ma.|||||
30708|Natalie Granite|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1729 +/- 5 Ma.|||||
30708|Natalie Granite|69591|5|Briefly described|p60|||Wonga Batholith.|1758 +/- 8 Ma (Pearson et al., 1992).||||Foliated biotite granite.|
30708|Natalie Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1758+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30708|Natalie Granite|72596|6|Mentioned|p2, p24|||Used by Geoscience Australia, 2011 (Sample ID 72205021) in reference to Wonga Granite[?].|1758+/-8 Ma|||||
30708|Natalie Granite|73137|5|Briefly described|p2, p5, p30-34|Statherian|Statherian|A sample of an unusual chalcopyrite-bearing leucocratic granite pod within an area of more strongly foliated granite yielded a magmatic crystallisation age of 1749 +/- 6 Ma, which matches the older extent of the Wonga Igneous Subprovince. [See article for field description, petrographic description and detailed geochronology].|1749 +/- 6 Ma||||Includes unusual chalcopyrite-bearing leucocratic granite.|11-OCT-22
30708|Natalie Granite|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP ages of 1758 +/- 8 Ma and 1729 +/- 5 Ma reported by Pearson et al. (1992).|1758 +/- 8 Ma|||||
30708|Natalie Granite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Leichhardt River Domain.|1729+/-5 Ma crystallisation age||||Felsic intrusives.|
30708|Natalie Granite|73553|4|Described|p18, p35-36, p44, p65, p72-73,|Statherian|Statherian|Mary Kathleen Domain. Wonga Igneous Subprovince. Named unit within the Wonga Belt but has not been previously described and did not appear on published maps, previously mapped as Wonga Granite subunit '3b'. Narrow, elongate unit ~35 km long and ~2.5 km wide, quality of outcrop is variable. Distribution presented here is a combination from Bastrakova et al., (2001) and detailed geological boundaries (GSQ, 2018). Maximum emplacement age of  1758+/-8 Ma U-Pb zircon SHRIMP (Pearson et al., 1992). White to bluish and yellow tones on radiometric images. Relatively low and bland magnetic response. Appears to intrude Argylla Formation. See also Natalie granite p88. See also p74 Tb 4.1.2, p78, p80-87. p91, p95, p101, p118, p247-249.|1729+/-5 Ma, 1749+/-6 Ma U-Pb zircon (SHRIMP)|||Faulted contact with Mount Maggie Granite in the west|Strongly foliated, porphyritic, biotite-amphibole monzogranite to syenogranite; local pegmatite; local mafic igneous bodies, biotite-rich domains.|03-FEB-23
26072|Nathan Group|14019|6|Mentioned|p14|||Possibly correlates with sedimentary units in the Victoria Basin.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|22453|6|Mentioned|p 12|||McArthur Basin||||||
26072|Nathan Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
26072|Nathan Group|22538|4|Described|p710, Fig4, p718|Calymmian||Part of the Favenc package.||||||26-MAR-18
26072|Nathan Group|22600|4|Described|Map legend|Calymmian|Calymmian|||||||
26072|Nathan Group|22644|5|Briefly described|3,5|||Geol. province: McArthur Basin.||||||20-JUL-06
26072|Nathan Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geo.l province: McArthur Basin||||||20-JUL-06
26072|Nathan Group|22664|6|Mentioned|34|Paleoproterozoic|Paleoproterozoic|Geol province McArthur Basin||||||07-NOV-08
26072|Nathan Group|22716|6|Mentioned|p236|||May be equivalent to the Birrindudu Group of the Birrindudu Basin.||||||
26072|Nathan Group|22808|6|Mentioned|7 fig 4|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|22853|5|Briefly described|23|Proterozoic|Proterozoic|Overlying unit: Roper Group, underlying unit: McArthur Group.||||||20-JUL-06
26072|Nathan Group|23216|6|Mentioned|p30||Statherian|Age: < 1640 Ma.||||||
26072|Nathan Group|23362|6|Mentioned|339 Fig.2|||||||||
26072|Nathan Group|23374|5|Briefly described|Fig3p5,34,35,6,18,29||Mesoproterozoic|Correlative of Mount Rigg Group. In the McArthur Basin.||||||20-NOV-06
26072|Nathan Group|23387|6|Mentioned|p18 fig.19|||||||||
26072|Nathan Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23395|6|Mentioned|p383|||||||||
26072|Nathan Group|23396|5|Briefly described|p 407 fig.2|||||||||
26072|Nathan Group|23398|5|Briefly described|p443|||||||||
26072|Nathan Group|23405|5|Briefly described|p594|||||||||
26072|Nathan Group|23407|5|Briefly described|p626|||||||||
26072|Nathan Group|23409|5|Briefly described|p536|||In the Isa Superbasin.||||||20-NOV-06
26072|Nathan Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
26072|Nathan Group|23776|5|Briefly described|p706|Calymmian|Statherian|Age 1615-1575 Ma.||||||20-JUL-06
26072|Nathan Group|23809|5|Briefly described|protero|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Bullita and Wattie Groups, and Lower Wade Creek Formation of the Victoria Basin.||||||22-NOV-04
26072|Nathan Group|23867|5|Briefly described|p14|Mesoproterozoic|Paleoproterozoic|Geological  Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23902|6|Mentioned|p1568 Fig.1|||Geological Province: McArthur Basin||||||
26072|Nathan Group|23910|4|Described|p290|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|23937|4|Described|p17, p24 Tb. 2|Calymmian|Statherian|Overlain by Phelp Sandstone; unconformably overlies the Vizard Group.  Age: 1614-1589Ma.  Type section in BAUHINIA DOWNS.  Geological Province: McArthur Basin.||||||18-APR-05
26072|Nathan Group|23963|6|Mentioned|p1238|||Geological Province: McArthur Basin.||||||10-MAR-05
26072|Nathan Group|24047|5|Briefly described|p12 Fig. 10, p11|Mesoproterozoic|Mesoproterozoic|Age: 1600-1570?Ma.  Overlies the McArthur Group.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|24048|4|Described|p64|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
26072|Nathan Group|24049|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||13-OCT-05
26072|Nathan Group|24050|5|Briefly described|p7|Mesoproterozoic|Paleoproterozoic|Age: 1589+/-Ma, 1613+/-4Ma.||||||07-NOV-08
26072|Nathan Group|24122|6|Mentioned|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|24297|5|Briefly described|p1|Proterozoic|Proterozoic|Possibly correlated with Wattie and Bullita Groups. Grological Province: McArthur Basin.||||||
26072|Nathan Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|40105|6|Mentioned|p310|||||||||
26072|Nathan Group|40109|5|Briefly described|p302|||||||||
26072|Nathan Group|40259|6|Mentioned|Table 1|||||||||
26072|Nathan Group|40691|3|Fully described|p11|||||||||
26072|Nathan Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|41019|5|Briefly described|p243|||||||||
26072|Nathan Group|41268|4|Described|p284|||||||||
26072|Nathan Group|41277|5|Briefly described|p80|||||||||
26072|Nathan Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|41721|5|Briefly described|p26, p27|||Includes the Balbirini Dolomite. Geological Province: McArthur Basin.||||||01-AUG-07
26072|Nathan Group|42385|4|Described|p23|||See also Table 4 p16.||||||20-NOV-06
26072|Nathan Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|42395|6|Mentioned|Fig.26 P86|||||||||
26072|Nathan Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||Includes: Dungaminnie Formation, Balbirini Dolomite and Smythe Sandstone.|Shown in legend as adjacent to Karns Dolomite. Underlies Lower Roper Group (Roper Group) units; overlies Batten Subgroup (McArthur Group) units.||07-NOV-11
26072|Nathan Group|42639|4|Described|p35, Table 6|||||||||
26072|Nathan Group|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
26072|Nathan Group|42739|5|Briefly described|map legend|Calymmian|Calymmian|Cyclic dolostone, dolarenite, sandstone, mudstone, evaporite casts, basic to intermediate volcanics, feldspathic sandstone, tuffite.||||||19-OCT-05
26072|Nathan Group|42812|3|Fully described|p42, Table 4|||||||||
26072|Nathan Group|42846|5|Briefly described|p503, Fig.1 p502|||Geological Province: McArthur Basin.||||||09-MAY-05
26072|Nathan Group|42935|6|Mentioned|p527|||||||||
26072|Nathan Group|43010|6|Mentioned|Table 14.|||||||||
26072|Nathan Group|43036|5|Briefly described|p55|||||||||
26072|Nathan Group|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26072|Nathan Group|43486|5|Briefly described|21|||||||||
26072|Nathan Group|43595|4|Described|p438||Mesoproterozoic|||||||
26072|Nathan Group|43788|6|Mentioned|p13||Proterozoic|||||||
26072|Nathan Group|44112|4|Described|p63,65|||Part of Supersequence 4||||||
26072|Nathan Group|45162|2|Defined|p136|Proterozoic|Proterozoic|Mention p45.||||||20-NOV-06
26072|Nathan Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-FEB-11
26072|Nathan Group|60483|4|Described|p7 Fig. 5, p9, p32|||Incl: Kookaburra Ck and Dungaminnie Fm, Mt Birch and Smythe Ssts, and Balbirini Dolomite. Unconform.over McArthur Gp.and under Roper Gp. Thickness: 700m. Geol.Prov: McArthur Basin. Correlates with Karns Dolomite.||||||05-OCT-07
26072|Nathan Group|60558|5|Briefly described|p7, p8 Fig. 6|Proterozoic|Proterozoic|Includes four units. Dominated by shallow water to locally emergent, often evaporitic carbonates with minor associated fine-grained shallow water clastics.||||||
26072|Nathan Group|60573|5|Briefly described|Map legend|Calymmian|Statherian|Includes Walmudga, Yalwarra, Kookaburra Creek Formations and Mount Birch Sandstone.  Overlain by Phelp Sandstone. Does not outcrop in the ROPER RIVER mapsheet area.||||||20-JUL-06
26072|Nathan Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|60682|6|Mentioned|p6|||Geological Province: Macarthur Basin.||||||
26072|Nathan Group|60685|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|61390|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
26072|Nathan Group|61403|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||
26072|Nathan Group|63112|6|Mentioned|p1190|||Southern McArthur Basin.||||||
26072|Nathan Group|63866|5|Briefly described|p113-p114, p116-p117, p123|||Walker Fault Zone, northern and central Caledon Shelf and Urapunga Fault Zone.|<1710 Ma (unit relationships)|||Unconformably overlain by the Roper Group. Unconformably overlies the West Branch Volcanics, Mount Bonner Sandstone and the Jalma Formation. Equivalent to the Mount Rigg Group.||
26072|Nathan Group|64724|5|Briefly described|p45 Fig.5, p46, 47|Calymmian|Statherian|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
26072|Nathan Group|64784|6|Mentioned|p3 Fig.3 |||||||||
26072|Nathan Group|64815|5|Briefly described|p3, p11, p13, p15 Fig.9 |Calymmian|Statherian|See also p16-18 Figs.10-12, p17, p19. Rawlings (1999) assigned the lower part of the Nathan Group to the McArthur Group.|1613 +/- 4 Ma and 1609 +/- 3 Ma.||Includes Balbirini Dolostone, Smythe Sandstone and Dungaminnie Formation.|Generally unconformably overlies the McArthur Group.|Dolostone; basal polymict conglomerate and pebbly lithic (chert) sandstone; beds of fine sandstone and siltstone.|
26072|Nathan Group|64816|6|Mentioned|p2 Fig.1, p4  |||||||||
26072|Nathan Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Balbirini Dolomite, Kookaburra Creek Formation, Mount Birch Sandstone, Dungaminnie Formation, Smythe Sandstone.|||
26072|Nathan Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|65228|4|Described|p7, p9, pp38-39, Fig.02.|Statherian|Statherian|McArthur Basin. Mixed carbonates and clastics. 1,200 m thick. Contains discontinuities.|1614-1610 Ma.||Includes Smythe Sandstone, Balbirini Dolomite and Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.||
26072|Nathan Group|65232|6|Mentioned|p5 Fig. 4|||Presented as Nathan and Mount Rigg groups on figure. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
26072|Nathan Group|65236|6|Mentioned|p4 Fig. 4|||Geological province: Beetaloo Sub-basin.||||||
26072|Nathan Group|65337|6|Mentioned|p7.||||c.1590 (Jackson et al. 2000b).|||||
26072|Nathan Group|65340|5|Briefly described|p57, p59, p10-11.|||Batten Trough. Possible partial correlation with Karns Dolomite, although characteristic pink tuffite beds of this unit have not been observed in the Karns Dolomite.|1589 +/- 3 Ma (Jackson et al. 2000b) medial Group.|||||26-MAR-18
26072|Nathan Group|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 437 m.||||Is overlain by Mantungula Formation.|Dolostone, chert, dolomitic sandstone, siltstone.|
26072|Nathan Group|66843|4|Described|p23-26, p34, p37-39|||Southern McArthur Basin. Composite stratigraphic column; gamma-ray curve. Lithofacies described in great detail, organised in 9 cycles. Evolution of the Group is revised in this study.|||Includes Balbirini Dolomite, Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.|A succession of stromatolitic carbonates with minor sandstone and shale.|12-SEP-19
26072|Nathan Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|McArthur Basin.|||Includes Balbirini Dolostone.|Overlies McArthur Group. Is overlain by Roper Group.||13-APR-12
26072|Nathan Group|67269|6|Mentioned|p20-21 Fig.19|||McArthur Basin.|||Dungaminnie Formation.|||
26072|Nathan Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p9|||NT (Jackson & Southgate 2000). Supersequences extend on to Lawn Hill Platform.|||Includes Yalwarra Volcanics and unconformity-bounded Lawn, Wide and Doom Supersequences.|||
26072|Nathan Group|67352|4|Described|v, p11,  p13 Tb.2, p51|Calymmian|Statherian|McArthur Basin. 1.6 km thick. Deposition terminated by Isan Orogeny.|1615-1575 Ma||Balbirini Dolostone, Smythe Sandstone.|Overlies McArthur Group paraconformably. Overlain by Roper Group (unconformably).|Dominated by stromatolitic and evaporitic dolostone; basal conglomerate and pebbly lithic sandstone.|
26072|Nathan Group|67564|5|Briefly described|p51.|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin. Correlative of Mount Rigg Group in Pine Creek Orogen.|1613 - 1590 Ma.|||||
26072|Nathan Group|68280|6|Mentioned|p26 fig 24|||McArthur Basin.|||Includes Dungaminnie Formation|||
26072|Nathan Group|69018|5|Briefly described|p450 Fig.1a, b|Calymmian|Statherian|Of McArthur Basin.|||Includes Balbirini Dolomite, Dungaminnie Formation.|||
26072|Nathan Group|69417|6|Mentioned|p2:5|Calymmian|Statherian|McArthur Basin.||||||12-JUL-16
26072|Nathan Group|69429|5|Briefly described|p14:3 Fig.14.4, 14:4|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Hosts quartz hematite (ironstone) lenses (the Murphys Fe prospect).|||Mount Birch Sandstone.|||12-JUL-16
26072|Nathan Group|69430|4|Described|p15:2-4, 9, 16, 19, 21-25, 27, 29-30, 61|||Jackson et al. (1987), for units overlying a regional unconformity within the upper part of the revised (Plumb and Brown, 1973) McArthur Group, but underlying the Roper Group. McArthur Basin. Fair to good conventional hydrocarbon reservoirs occur.|||Balbirini, Karns Dolostones; Mount Birch, Smythe Sandstones; Knuckey, Walmudga, Dungaminnie Formations; Yalwarra Volcanics.|Unconformably overlies Amos Formation (Batten Subgroup, McArthur Group), Bath Range Formation (Balma Group), Vizard and Tawallah Groups. Is overlain unconformably by Roper Group.|Includes a relatively thin and lenticular basal siliciclastic and often conglomeratic unit, overlain by thicker carbonate and siliciclastic rocks.|12-JUL-16
26072|Nathan Group|69591|6|Mentioned|p47|||Northern Territory. Includes the Term, Lawn, Wide and Doom Supersequences.||||||
26072|Nathan Group|69673|4|Described|vii, p3 fig 2, p15, p32, p41|Paleoproterozoic|Paleoproterozoic|Fair to good conventional reservoir properties.|||Includes Balbarini Dolostone, Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Smythe Sandstone, Dungaminnie Formation, Karns Dolostone|Unconformably overlies McArthur Group|Basal fluvial chert-clast sandstone overlain by stromatolitic and ooidal dolostone; minor siliciclastic sandstone.|
26072|Nathan Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic||1589 +/- 3 Ma.|||Overlies McArthur Group. Overlain unconformably by Phelp Sandstone (Roper Group).||
26072|Nathan Group|70897|5|Briefly described|p42-45|||Correlated with upper part of South Nicholson Group. Uppermost units deposited c.1590 Ma.|||Dungaminnie Formation, Balbirini Dolomite.|Is overlain unconformably by Roper Group.|Tightly folded and faulted carbonate-rich succession.|
26072|Nathan Group|70968|5|Briefly described|p2 Fig.3,p6-8,p10,p13,p123,p132,p138-139|Calymmian|Statherian|On detrital zircon and lithological grounds, doubt is cast on the general acceptance of equivalence of this unit with Bullita and Wattie Groups. SHRIMP U-Pb zircon age of a tuff in the upper part of the Group.|1589 +/- 3 Ma (Page et al., 2000).||Walmudga Formation.|Is overlain unconformably by Phelp or Limmen Sandstones (Roper Group).||
26072|Nathan Group|71059|5|Briefly described|p1-3, p7|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Phelp Sandstone (Roper Group). Equivalent to Wattie and Bullita Groups (Birrindudu Basin).||
26072|Nathan Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p6, p18, p30, p33|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.|||Includes the Smythe Sandstone, Balbirini Dolostone and Karns Dolostone.|Overlies the McArthur Group, Habgood Group and Balma Group. Equivalent to the Bullita and Wattie Groups.||
26072|Nathan Group|71488|6|Mentioned|p141 fig 1b|Mesoproterozoic|Mesoproterozoic|||||Unconformably overlain by the Roper Group.||
26072|Nathan Group|71606|5|Briefly described|p135,137-138|Calymmian|Calymmian|Walker Trough, Caledon Shelf, Bauhinia Shelf and Batten Trough; McArthur Basin. Evaporite-carbonate sequence deposited in a broad sag basin across most of the region with no evidence of tectonic control from previous rifts. Correlable to Mount Rigg Group and Karn Dolomite.||||Overlain unconformably by Roper Group. Underlain unconformably by Balma Group, Vizard Formation, Spencer Creek Group, Tawallah group and McArthur Group.||
26072|Nathan Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Includes Yalwarra Volcanics.||Cyclic coarse-grained evaporitic-stromatolitic-ooidal dolostone, sandstone, siltstone; minor conglomerate; synsedimentary basaltic sills, sandstone, mudstone (Yalwarra Volcanics).|05-MAR-20
26072|Nathan Group|71779|5|Briefly described|p5|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.||||Disconformably or unconformably overlain by the Roper Group.||
26072|Nathan Group|71893|4|Described|p9, p13|Calymmian|Calymmian|McArthur Basin. SHRIMP age is derived from a tuff in this unit.|1589 +/-3 (SHRIMP, Page et al, 2000)||Includes the Walmudga Formation.|Unconformably overlain by the Phelp Sandstone and the Limmen Sandstone (Collara Subgroup) .||
26072|Nathan Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Dolostone with lesser sandstone and fine-grained clastics.|
26072|Nathan Group|72373|5|Briefly described|iii,p1-2,37-28,33,36,39|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Smythe Sandstone, Balbirini Dolostone, Knuckey Formation and Mount Birch Sandstone.|Underlain by Balma Group.||
26072|Nathan Group|72377|5|Briefly described|p13|Mesoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Balbirini Dolostone.|||10-OCT-19
26072|Nathan Group|72381|5|Briefly described|p772|||Of [or under?] Beetaloo Sub-basin, McArthur Basin.||||Overlain unconformably by Cororan Formation.||03-OCT-19
26072|Nathan Group|72523|5|Briefly described|piii, p1, p1 Fig.1, p2 Fig.2, p8, p12.|Early Mesoproterozoic|Early Mesoproterozoic|Described as part of the Favenc package (Rawlings 1999).|||Includes Smythe Sandstone, Balbirini Dolostone, Dungaminnie Formation and Knuckey Formation.|Unconformably overlies Amos Formation, McArthur and Tawallah groups. Unconformably overlain by Roper Group.||
26072|Nathan Group|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin. Part of the Favenc package (Lithostratigraphic package).|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Balbirini Dolostone, Smythe Sandstone, Dungaminnie Formationh and Karns Dolostone.|Shown as overlying Vizard Group, McArthur Group and shown as unconformably underlying Roper Group.||
26072|Nathan Group|72527|6|Mentioned|p10.|Paleoproterozoic|Paleoproterozoic|Dating of this group has assisted in constraining maximum depositional ages for the South Nicholson Group.|||Includes Balbirini Dolostone.||Includes tuffs.|
26072|Nathan Group|72718|6|Mentioned|piii, p5-9|Mesoproterozoic|Mesoproterozoic|Beetaloo Sub-basin, McArthur Basin. Isa Superbasin, Favenc package. A tuff in the upper portion of the group yielded a SHRIMP U-Pb zircon age of 1589 +/- 3 Ma.|||Wakmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone.|Unconformably underlain[?] by Nagi Formation (Vizard Group). Unconformably overlain by Phelp Sandstone and[?] Mantungula Formation (both of Collara Subgroup, Roper Group).||
26072|Nathan Group|72912|5|Briefly described|p5 Fig.3, p18.|Calymmian|Statherian|This group extends across all of the  Southern McArthur Basin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Balbirini Dolostone, Smythe Sandstone and Karns Dolostone.|Unconformably underlies Roper Group and unconformably overlies Vizard and McArthur Groups.||
26072|Nathan Group|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Upper Balbirini Dolostone, Smythe Sandstone, Karns Dolostone.|Unconformably underlain(?) by Vizard Group and McArthur Group. Unconfrmably overlain by Roper Group.||
26072|Nathan Group|73242|6|Mentioned|p39|||||||Overlain by[?] Phelp Sandstone, Collara Subgroup, Roper Group.||
26072|Nathan Group|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
26072|Nathan Group|73412|4|Described|p2, 4, 6, 8, 10-11, 13, 15-19|||Southern McArthur Basin. Dry bulk density tabulated.|c.1610-1580 Ma.||Smythe Sandstone, upper Balbirini Dolostone, Dungaminnie Formation, Karns Dolostone.|Unconformably overlies McArthur and (locally) Tawallah Groups. Is overlain unconformably by Roper Group.|Siliciclastic and carbonate rocks with minor intercalated mafic volcanics.|
29341|Native Creek Microgranite|22845|6|Mentioned|p57||Triassic|||||||
29341|Native Creek Microgranite|22846|2|Defined|p6,65-6|Middle Triassic|Carboniferous|Intruded by Calgoa Diorite.||||||
29341|Native Creek Microgranite|43588|6|Mentioned|p30|Late Triassic|Early Triassic|||||||
29341|Native Creek Microgranite|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
29341|Native Creek Microgranite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
29341|Native Creek Microgranite|68679|5|Briefly described|p409, p411|Late Triassic|Late Triassic|Northern New England Orogen. Outcrop area ~6 km2.||Station Creek Igneous Complex.||Is intruded by Calgoa Diorite.|Hornblende-biotite microgranite; subequigranular to porphyritic.|
79789|Nebine Metamorphics|71251|4|Described|p2-3, p8-9, p11, p13, p20, p24, p48|||Thomson Orogen. Multiply-deformed metasedimentary rocks (greenschist) forming an extensive, geophysically-bland basement to the Eromanga Basin. Core and thin-section photographs. Has an elevated and highly variable natural gamma signal. HyLogger data.|~520 Ma (Kositcin et al., 2015).|||Is overlain by Cadna-owie Formation.|Green quartz-muscovite-biotite-chlorite schist (topmost 35m strongly weathered). Quartz commonly forms irregular milky segregations up to 5cm in diameter, often with some albite. Grain size variation in psammitic layers with larger grains is ~1mm.|
79789|Nebine Metamorphics|71864|6|Mentioned|p3-p4|||||||||
79789|Nebine Metamorphics|71965|4|Described|p896,899,903-904,906-908,910-913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Occurs adjacent Werewilka Formation. Generally low and featureless in magnetic response with some broad magnetic striping. Age constraints: 520+\-10 Ma (MDA); 435+\-3 Ma (Minimum DA, overlying sediments). Possible "on-strike" stratigraphic equivalent to Werewilka Formation, separated by the Caiwarro Fault Zone.|520+\-10 Ma (MDA)|||Correlable with Warratta Group, Tongo Formation, Twin Tanks Metamorphics, Thomson beds, Werewilka Formation.|Biotite-muscovite phyllite and garnet-plagioclase-muscovite-biotite-quartz schist, laminated quartz-mica schist, locally up to amphibolite facies.|29-OCT-19
79789|Nebine Metamorphics|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Thomson Orogen. Intersected in GSQ Mitchell 1 drillhole, samples analysed yielded a maximum depositional age of c. 520 Ma|<520 Ma|||||
79789|Nebine Metamorphics|72522|4|Described|p1-2, p33, p41-48|Cambrian|Cambrian|Very similar lithology to the Glenroy Formation except slightly higher metamorphic grade and multiple deformation fabrics exist in this unit. Dated sample is lower metamorphic grade than Nebine Metamorphics further north and may represent a younger unit. Nebine Metamorphics also identified in AOP Alba 1, GSQ Mitchell (MDA ~520 Ma), along the Nebine Ridge. Date ref. Kositcin et al., 2015; Purdy et al., 2016.|435+/-4 Ma U-Pb SHRIMP max.dep.||||Includes siltstone sampled for dating; quartz-muscovite-biotite-chlorite schist in GSQ Eulo 1.|
79789|Nebine Metamorphics|73600|6|Mentioned|p202, p204|||||||||
36248|Neds Gully Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36248|Neds Gully Granite|60425|4|Described|p286-7 Appdx|Late Carboniferous|Late Carboniferous|Of Ravenshoe Suite (O'Briens Creek Supersuite). Porphyritic biotite granite. Informally referred to as Pinnacles porphyry. I-type.||||||07-FEB-11
39850|Nested Rhyolite Porphyry|24485|5|Briefly described|p50 Tb.8|Late Carboniferous|Late Carboniferous|||||||
39850|Nested Rhyolite Porphyry|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
39850|Nested Rhyolite Porphyry|24487|5|Briefly described|Map legend|||||||||
27860|Nettle Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 313 +/- 4Ma, Rb-Sr.||||||
27860|Nettle Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
27860|Nettle Granite|40743|6|Mentioned|Fig.2|||||||||
27860|Nettle Granite|41740|6|Mentioned|p222|||||||||
27860|Nettle Granite|41824|6|Mentioned|p201|||||||||
27860|Nettle Granite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
27860|Nettle Granite|60425|4|Described|p286-7 Appdx., p285|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Ck Supersuite).Includes Devon+ Shady Microgranites on most maps.Ages: 303Ma,308+/-4Ma, 311+/-4Ma, 313+/-4Ma, 315 Ma.Med.-gr., slightly-highly porphyritic biotite granite: 4 phases recognised; +assoc'd Sn mineralisation.  I-type||||||07-FEB-11
28005|Nettle Suite|23291|5|Briefly described|p96 Tb. 3.11|Late Carboniferous|Late Carboniferous|Parent: O'Brien's Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
28005|Nettle Suite|23423|5|Briefly described|p241||Carboniferous|Age: ~308-315 Ma. O'Briens Creek Supersuite. Kennedy Igneous Province.||||||
28005|Nettle Suite|23446|6|Mentioned|p448 Fig.1|||||||||
28005|Nettle Suite|23616|5|Briefly described|p75|||Rb-Sr total rock age 310 Ma. Also see Table 5 p70. Of O'Briens Creek Supersuite. Coolgarra Batholith.||||||
28005|Nettle Suite|43060|6|Mentioned|p101|||of O'Briens Creek Supersuite||||||
28005|Nettle Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of O'Briens Creek Supersuite.||||||15-JUN-06
28005|Nettle Suite|60425|5|Briefly described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of the O'Briens Creek Supersuite. Formerly the Emu Suite of Pollard (1984, 1988; Witt 1985). Contains 25 named granites.||||||07-FEB-11
28005|Nettle Suite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.|||I-type.|
31382|Neurum Complex|22846|1|Redefined|p6,42-5,77|Late Triassic|Late Triassic|Contains 10 different rock types and supersedes several previous names such as Neurum Granite/Tonalite and Woodford Granite..||||||
31382|Neurum Complex|23609|4|Described|p7-10|||Probably abbreviation of Neurum Igneous Complex. I-Type characteristics. North D'Aguilar Block.||||||
31382|Neurum Complex|23799|5|Briefly described|p115 Fig. 10|Triassic|Permian|Geological Province: D'Aguilar Subprovince.||||||
31382|Neurum Complex|43588|6|Mentioned|p31|Late Triassic|Early Triassic|Variation on Neurum Tonalite||||||
31382|Neurum Complex|44925|5|Briefly described|Map Legend||Late Triassic|||||||
31382|Neurum Complex|68679|5|Briefly described|p326-327, p330-331, p387, p427-428, p436|Late Triassic|Late Triassic|Sunshine Coast hinterland. Previously the Neurum Tonalite. Mainly metaluminous I-type. Possibly comagmatic with the adjacent Bellthorpe Andesite which this unit largely surrounds.|227.7 Ma (K-Ar: Webb and McDougall, 1967).|||Intrudes the Rocksberg Greenstone, Booloumba and Cambroon beds, Jimna Phyllite, Cedarton Volcanics and Peters Creek Greenstone.|Mainly equigranular to porphyritic granodiorite, with granite ranging through to quartz monzodiorite and quartz diorite. 10 different rock types occur, not individually mapped. High-level emplacement.|
79747|Nevada granodiorite|70673|4|Described|p5-6, p10, p116-120|Permian|Permian|Nevada station, c.43 km W of Bowen. Forms prominent, massive and unfoliated, outcrops: relict boulders, tors and whalebacks. Age is of magmatic crystallisation.Abbreviated to Nevada GD on p6. Shown as 'Nevada granodiorite' p5, p116.|297.8 +/- 1.6 Ma U/Pb SHRIMP|||Is possibly intruded by dykes of Mount Abbot Igneous Complex.|Pale grey, mainly medium-grained, slightly porphyritic biotite-hornblende granodiorite, with scattered mafic inclusions. Cut by granite dykes up to 15m thick.|24-MAR-17
80509|New Hope Sandstone Member|72889|4|Described|p2-3, p33, p38-p40 Fig 2.7, p42-p44.|Statherian|Statherian|From the western limb of the Mort River Anticline, and stratigraphically underlies the upper Starcross Formation sample that yielded the 1679 +/- 11 Ma maximum depositional age. However, these calculated maximum depositional ages are within uncertainty of one another. Previously New Hope Sandstone, see p5, p8. Refer to 1:250 000 sheet DUCHESS (SF5406). Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results. See also p47, p54.|1662+/-22 Ma max. dep. age.|Starcross Formation||Grades into Starcross Formation on lower and upper boundaries and is laterally discontinuous.|Includes medium to coarse-grained, thick to very thickly bedded, sub-feldspathic sandstone.|25-NOV-20
26077|New Moonta Diorite|24382|5|Briefly described|Map legend|Triassic|Triassic|||||||
26077|New Moonta Diorite|41778|2|Defined|Table 2|Middle Triassic|Early Triassic|Reserved as New Moonta.||||||14-AUG-08
26077|New Moonta Diorite|42054|6|Mentioned|p272|||||||||
26077|New Moonta Diorite|43008|5|Briefly described|map legend|||||||||
26077|New Moonta Diorite|63821|5|Briefly described|p30|Middle Triassic|Early Triassic|Age: 232+/-4Ma. Hornblende-pyroxene diorite and hornblende-pyroxene quartz diorite. Intrudes sediments of Curtis Island Group; intruded by Wonbah Granodiorite. Host to numerous porphyry intrusive related gold deposits.||||||07-FEB-11
26077|New Moonta Diorite|64556|5|Briefly described|p29-32, p56|Late Permian|Late Permian|Age of magmatic emplacement: 269.2+/-1.6Ma. Age analysis details included. Sample analysed was from the type locality - massive equigranular biotite-hornblende-titanite quartz diorite.||||||07-FEB-11
26077|New Moonta Diorite|65452|5|Briefly described|p7 Tb.2|Cisuralian|Guadalupian|SHRIMP U-Pb zircon magmatic crystallisation age.|269.2 +/- 1.6 Ma (Carson et al. 2006).||||Equigranular biotite-hornblende-titanite quartz diorite.|
26077|New Moonta Diorite|68421|5|Briefly described|Map Legend|Roadian|Wordian|Age determined a site on the Mount Perry sheet area.|269.2 +/- 1.6 Ma||||Biotite-pyroxene diorite, hornblende-pyroxene quartz diorite.|
26077|New Moonta Diorite|68679|5|Briefly described|p421, p430|Permian|Permian|Gayndah-Gladstone belt. Previously (Ellis, 1968) mapped as part of the Hogback Tonalite; removed/renamed after dating (Carson et al., 2006) showed it was Permian.|269.2 +/- 1.6 Ma (SHRIMP: Carson et al., 2006).||||Biotite-pyroxene diorite, hornblende-pyroxene quartz diorite.|
26077|New Moonta Diorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|269+/-1.6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Diorite.|
26077|New Moonta Diorite|73197|6|Mentioned|p476 Fig.7, p477|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase.|269 or 268 Ma U-Pb||||Mafic intrusives.|
22537|Newburgh Granodiorite|23032|5|Briefly described|p40|||||||||
22537|Newburgh Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
22537|Newburgh Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
22537|Newburgh Granodiorite|43480|2|Defined|7-64|Devonian|Silurian|||||||
22537|Newburgh Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Buff to grey, subequigranular, muscovite-biotite granodiorite with sparse schlieren and very sparse to rare feldspar phenocrysts to 1.5 cm.|
22537|Newburgh Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Buff to grey, subequigranular, muscovite-biotite granodiorite with sparse schlieren and very sparse to rare feldspar phenocrysts to 1.5 cm.|
22537|Newburgh Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
26805|Newcastle Range Volcanic Group|22669|6|Mentioned|P259||Visean|Age of unit is 327+/-4 Ma||||||
26805|Newcastle Range Volcanic Group|23032|6|Mentioned|p45|||||||||
26805|Newcastle Range Volcanic Group|23291|3|Fully described|p40, p95 Tb. 3.10|Permian|Carboniferous|Geological Province: Georgetown Region.||||||07-JUL-15
26805|Newcastle Range Volcanic Group|23430|5|Briefly described|p490|||||||||
26805|Newcastle Range Volcanic Group|23453|5|Briefly described|p14|Namurian|Visean|~325+/-5Ma||||||
26805|Newcastle Range Volcanic Group|23497|6|Mentioned|p32||Permian|||||||
26805|Newcastle Range Volcanic Group|23510|5|Briefly described|Map Legend||Early Permian|||||||
26805|Newcastle Range Volcanic Group|23619|4|Described|p31 table 1||Carboniferous|Previously named Newcastle Range Volcanics. 327+/-4Ma. Underlain by the Gilberton Formation.||||||
26805|Newcastle Range Volcanic Group|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26805|Newcastle Range Volcanic Group|40860|5|Briefly described|p115|||||||||
26805|Newcastle Range Volcanic Group|40960|6|Mentioned|p228|||||||||
26805|Newcastle Range Volcanic Group|41675|6|Mentioned|p76|||||||||
26805|Newcastle Range Volcanic Group|41680|5|Briefly described|p106|||||||||
26805|Newcastle Range Volcanic Group|43113|4|Described|Table 1 p18||Carboniferous|||||||
26805|Newcastle Range Volcanic Group|43253|5|Briefly described|map legend||Carboniferous|||||||
26805|Newcastle Range Volcanic Group|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
26805|Newcastle Range Volcanic Group|43664|6|Mentioned|p80|||||||||
26805|Newcastle Range Volcanic Group|43716|6|Mentioned|p21|||||||||
26805|Newcastle Range Volcanic Group|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Consists of: Eveleigh Volcanic Subgroup, Kungaree Volcanic Subgroup, Wirra Volcanic Subgroup.||||||
26805|Newcastle Range Volcanic Group|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Includes the Wirra Volcanic Subgroup, Eveleigh Volcanic Subgroup, Canyon Dacite.||||||
26805|Newcastle Range Volcanic Group|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Includes: Eveleigh Volcanic Subgroup, Nammarong Volcanic Subgroup.||||||19-AUG-04
26805|Newcastle Range Volcanic Group|66529|6|Mentioned|p60 |||Has high prospectivity for orthomagmatic U mineralisation; is associated with several small U deposits.||||||
26805|Newcastle Range Volcanic Group|68307|5|Briefly described|p78, p88|Permian|Carboniferous|Thomson Orogen.||||||
26805|Newcastle Range Volcanic Group|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||Includes Wirra and Eveleigh Volcanic Subgroups.||Mainly rhyolitic ignimbrite.|
26805|Newcastle Range Volcanic Group|68354|5|Briefly described|Map legend.||Early Carboniferous|Kennedy Province. Min age: Early Permian?|||Includes Wirra, Eveleigh, Kungaree and [misspelled] Nammarong Volcanic Subgroups and Cumbana Rhyolite.||Mainly rhyolitic ignimbrite.|08-JUL-15
26805|Newcastle Range Volcanic Group|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||Includes Eveleigh Volcanic Subgroup and Nammarong Volcanic Subgroup.|||
26805|Newcastle Range Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|Parts of this unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk. See also CPvk.||||||30-APR-13
26805|Newcastle Range Volcanic Group|68576|5|Briefly described|Q_11: p21-23, p27, p31|Carboniferous|Carboniferous|One of the most extensive remnants of Carboniferous extrusive rocks in north Queensland. Forms the Newcastle Range. Subaerial eruption and emplacement.|||Wirra, Kungaree, Namarrong, Eveleigh, Volcanic Subgroups.||Predominantly ignimbrite. Minor lava: rhyolites (85-90%), dacites (5-10%); the remainder andesite. Intercalated sedimentary rocks are fluviatile, shallow lacustrine, or mass-flow in origin.|
26805|Newcastle Range Volcanic Group|69591|5|Briefly described|p102|Carboniferous|Carboniferous|||||Overlies Gilberton Formation.||
26805|Newcastle Range Volcanic Group|69593|4|Described|p485, p487 Fig.6.9, p488-491, p512-513|Permian|Late Carboniferous|Tate and Kidston Subprovinces, Kennedy Igneous Association. Outcrop area is ~2,500 km2 in the N-aligned Newcastle Range, Kidston Subprovince. The A-type units are thought to be younger (Permian). Sm-Nd isotope data tabulated.|~330-325 Ma (I-types: Black and McCulloch, 1990).||Eveleigh, Namarrong, Volcanic Subgroups; Jinker Creek, Mosaic Gully, Bousey, Brodies Gap Rhyolites.||Rhyolite (~85-90%), dacite (5-10%), andesite and rare basalt. Dominantly I-type, with A-type magmatism in the north.|
26805|Newcastle Range Volcanic Group|70207|5|Briefly described|p4, p14, p81-82|Permian|Carboniferous|Forms most of the Newcastle Range NE of Georgetown: extends over ~2,500 km2. Maximum preserved thickness of ~8,000-10,000m. Comprises 15 Formations. Previous age determinations discussed.|||Namarrong, Wirra, Eveleigh, Kungaree, Volcanic Subgroups.|||
28097|Newirie Formation|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
28097|Newirie Formation|22781|4|Described|p20|Proterozoic|Proterozoic|Holroyd Group||||||
28097|Newirie Formation|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group, Coen Inlier. Thickness 3000m||||||
28097|Newirie Formation|43596|4|Described|p19 Tb. 1, p23|Mesoproterozoic|Mesoproterozoic|Of Holroyd Gp. Max.thickness: 3000m. Thin-bedded slate, sandy slate, metasst.; qrtzite in SE; locally tourmaline-mica schist. Incl'd in "claystone sequence C" by Marjibanks (1980). Conf. below Gorge Fm;prob'ly interfingers with Carysfort Quarztite below.||||||07-APR-15
28097|Newirie Formation|43738|6|Mentioned|p49|||||||||
28097|Newirie Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||24-JAN-05
28097|Newirie Formation|69591|5|Briefly described|p76 Fig.2.74, p78 Tb.2.6|||Savannah Province, Coen Inlier. 3000m thick. Occurs mostly N and W of Coleman River.||Holroyd Group.||Interfingers with Carysfort Quartzite.|Thin-bedded slate, sandy slate amd metasandstone, phyllite, quartzite, schist.|
30724|Nicholson Suite|24197|4|Described|p22, p93|||Example of the Nicholson Association. Predominantly felsic and comprises Nicholson Granite and its comagmatic volcanics, the Cliffdale Volcanics. Geological Province: Murphy Inlier, Mount Isa Inlier.||||||07-FEB-11
30724|Nicholson Suite|50536|5|Briefly described|p1.2, 1.4, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1850Ma.||||||07-NOV-08
30724|Nicholson Suite|50605|6|Mentioned|p3.1, 7.1|||Geological Province: Mount Isa Inlier.||||||
30724|Nicholson Suite|65396|6|Mentioned|p301|||See Nicholson Granite. Considered by Budd et al. (2002) to have little or no metallogenic potential in the Mount Isa Inlier.||||||
30724|Nicholson Suite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|||See also p9, p107.|||Includes Nicholson Granite Complex.|||
30724|Nicholson Suite|68542|6|Mentioned|p1 |||||||||
30724|Nicholson Suite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
30724|Nicholson Suite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
30724|Nicholson Suite|69591|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|||||||
23874|Nightflower Dacite|23422|5|Briefly described|Plate 7.3|Late Carboniferous|Late Carboniferous|||||||
23874|Nightflower Dacite|23423|4|Described|p307 Table 7.3||Late Carboniferous|Age: 308 +/- 4 Ma (Rb-Sr). Featherbed Volcanic Group.||||||
23874|Nightflower Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V116. Assumed to be I-Type.||||||
23874|Nightflower Dacite|23616|6|Mentioned|Table 3 p46|||||||||
23874|Nightflower Dacite|23713|4|Described|p22, 24||Late Carboniferous|Age: 308+/-4 Ma (Rb-Sr). I-type characteristics. Of Featherbed Volcanic Group. O'lying unit Nychum Volcanics - disconformable or unconformable. Underlying unit  Hodgkinson Fm - unconformable.||||||
23874|Nightflower Dacite|42681|5|Briefly described|p19|||||||||
23874|Nightflower Dacite|43083|5|Briefly described|p91|||Of Featherbed Volcanic Group Age: 308+/-4 Ma (Rb-Sr). Unconformably overlies Hodgkinson Formation; disconformably overlain by Nychum Volcanics; faulted against Featherbed Volcanic Group.||||||17-JUN-09
23874|Nightflower Dacite|43087|5|Briefly described|p90|||Of Featherbed Volcanic Group. Rb-Sr biotite age of 308+/-4 Ma.||||||
23874|Nightflower Dacite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Dacitic to rhyodacitic ignimbrites, variously welded (intensely, moderately, poorly),; conglomerate to breccia.  Age: 309+/-4Ma.||||||15-JUN-06
23874|Nightflower Dacite|43254|5|Briefly described|map legend||Late Carboniferous|Age 308+/-4 Ma.||||||
23874|Nightflower Dacite|43259|4|Described|Appendix 1,p12.||Late Carboniferous|of Featherbed Volcanic Group. Age is 308+/-4 Ma.||||||
23874|Nightflower Dacite|43285|5|Briefly described|Map Legend||Late Carboniferous|||||||
23874|Nightflower Dacite|43567|6|Mentioned|Fig.2,p398||Late Carboniferous|||||||
23874|Nightflower Dacite|43625|4|Described|p36|||Age: 308+/-4 Ma||||||
23874|Nightflower Dacite|43626|2|Defined|p34||Late Carboniferous|Age: 308+/-4 Ma||||||22-APR-09
23874|Nightflower Dacite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Age: 308 +/- 4 Ma (Rb-Sr). Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||31-MAY-04
23874|Nightflower Dacite|60425|3|Fully described|p45 and 48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Four informal subunits. Unconformably overlain by Nychum Volcanics; unconformable on Hodgkinson Fm. Cut by Bilch Ck Granodiorite and Wabaredory Granite. Age: 308+/-4Ma (Rb-Sr). Thickness: ~300m? Lithological detail given.||||||07-FEB-11
23874|Nightflower Dacite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|308 Ma.|Featherbed Volcanic Group.||||
37039|Ninderry Rhyolite|23251|6|Mentioned|Table 1 p8|||Conformably overlies Carol Creek Rhyolite. Misspelling of Ninderry Member?||||||21-JUN-06
37039|Ninderry Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.|217 +/- 2 Ma (K-Ar whole rock for altered rock).|North Arm Volcanic Group.|||Variably flow-banded, sparsely phyric rhyolite and rhyodacite lavas; phenocrysts of oligoclase, aegerine augite and rare quartz; autobreccia and mesobreccia lenses or thin clay layers between flows (flows 15-50m thick). Local hydrothermal alteration.|
37039|Ninderry Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
41094|Nine Mile Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41094|Nine Mile Granite|65388|2|Defined|p269, p236 Fig. 81, p256, 273|Early Permian|Late Carboniferous|Intrudes Torsdale Volcanics, Glen View Quartz Monzodiorite, and probably Rockdale Granite. High-level intrusion, possibly related to Torsdale Volcanics. Not isotopically dated. Tentative age assigned. Mainly pale pink to dark reddish pink, pale brown or, rarely, pale grey, fine to medium-grained, slightly porphyritic, leucocratic biotite granite.||||||
41094|Nine Mile Granite|68679|5|Briefly described|p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Possibly comagmatic with Torsdale Volcanics.||||Intrudes Torsdale Volcanics, Glen View Quartz Monzodiorite, and probably Rockdale Granite.|Pink to dark reddish pink, pale brown or rarely pale grey, fine- to medium-grained, slightly porphyritic leucocratic biotite granite; slightly to moderately altered. High-level.|
75151|Ninian Bay Suite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains the informally named Ninian Bay microgranite. S-type.||||||07-FEB-11
30187|Ninian Bay granite|43111|4|Described|p25|||Informal 'definition'.||||||21-APR-09
75152|Ninian Bay microgranite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Informal name. Of Ninian Bay Suite (Cooktown Supersuite). S-type. Fine- to medium-grained, slightly porphyritic to seriate biotite granite; accessory tourmaline, altered cordierite? (rare); tourmaline-rich clots common.||||||07-FEB-11
36167|No Hays Minas Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36167|No Hays Minas Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36167|No Hays Minas Granite|60425|4|Described|p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pink, coarse-grained, seriate biotite granite. Included in Oakey Granite on most recent maps. I-type.||||||07-FEB-11
41801|Nob Creek Amphibolite|60481|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|Of the Marlborough Metamorphics. Fine to medium grained schistose amphibolite interbedded with minor quartz-mica-feldspar schist; minor stratiform massive sulphide.||||||07-NOV-08
41801|Nob Creek Amphibolite|61035|5|Briefly described|p17|||Of the Marlborough Metamorphics. Prominent amphibolite unit, hosts a minor base-metal mineralisation. Geological Province: Marlborough Block, Wandilla Province.||||||07-FEB-11
41801|Nob Creek Amphibolite|65388|5|Briefly described|p153-154, p70, 150||Late Devonian|Of Marlborough Metamorphics?, Marlborough Block. Age possibly Late Devonian. Described by Muscio (1994), Paterson (1994). Used informally by Harbort (2001) for the prominent amphibolite that is associated with base metal mineralisation at the Nob Creek prospect NE of Marlborough. Mostly dark green, fine-grained and well-foliated and strongly lineated. Mainly nematoblastic actinolite or hornblende and albite with minor quartz, epidote, titanite and opaques. No relict mineralogy preserved. Foliation defined by alternating albite and amphibole layers. Represents submarine basaltic lava in a sequence of cherty pelitic sediments.||||||
41801|Nob Creek Amphibolite|68679|5|Briefly described|p308|||Withnall et al. (2009). Marlborough Block. Forms a narrow band up to 300m wide and 6km long. Associated with base metal mineralisation at the Nob Creek prospect.||Marlborough Metamorphics.|||Foliated and lineated amphibolite; metamorphosed submarine, subalkaline, tholeiitic basalt.|
76896|Nobbs Tank Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event.||Sybella Suite|||Pink gneissic granite.|
76896|Nobbs Tank Granite|69591|5|Briefly described|p59|||Maramungee area.|||||Pink gneissic granite.|
79956|Noccundra Granite|71965|6|Mentioned|p911|||Geological province: Thomson Orogen. Of Ella Belt.||||||
23875|Noel Micromonzonite|23291|5|Briefly described|p50, p91 Tb. 3.9, p98 Tb. 3.11|Late Carboniferous|Carboniferous|Intrudes the Butlers Volcanic Group. Geological Province: Georgetown Region.||||||11-MAY-15
23875|Noel Micromonzonite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 33.  Assumed to be I-Type.||||||
23875|Noel Micromonzonite|23619|4|Described|p40 Table 2||Carboniferous|Intrudes McLennons Creek Rhyolite and Sues Creek Microgranite.||||||
23875|Noel Micromonzonite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23875|Noel Micromonzonite|40542|6|Mentioned|p97|||||||||
23875|Noel Micromonzonite|43113|4|Described|Table 2 p25||Carboniferous|||||||
23875|Noel Micromonzonite|43253|5|Briefly described|map legend||Carboniferous|||||||
23875|Noel Micromonzonite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
23875|Noel Micromonzonite|43740|4|Described|p29||Carboniferous|||||||
23875|Noel Micromonzonite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23875|Noel Micromonzonite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Unit in Lochaber Ring Structure.|||||Grey hornblende-augite quartz-micromonzonite.|
23875|Noel Micromonzonite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Biotite-hornblende-augite micromonzonite, diorite. I-type.|
36490|Noname Creek complex|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 75.||||||
24432|Nonda Granite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Fine to very fine-grained melanocratic biotite granite, granodiorite, microgranite. Overlies Esmeralda Granite.||||||13-MAY-15
24432|Nonda Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|melanocratic biotite granite, granodiorite, microgranite.||||||02-JUL-04
24432|Nonda Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||13-MAY-15
24432|Nonda Granite|23430|6|Mentioned|p456.|||||||||
24432|Nonda Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 809. ?S-Type.||||||
24432|Nonda Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
24432|Nonda Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24432|Nonda Granite|40659|6|Mentioned|p250|||||||||
24432|Nonda Granite|40954|6|Mentioned|p133|||||||||
24432|Nonda Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
24432|Nonda Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
24432|Nonda Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Fine to very fine-grained, melanocratic biotite granite, granodiorite, microgranite.||||||
24432|Nonda Granite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Fine- to very fine-grained melanocratic biotite granite, granodiorite, microgranite.|
24432|Nonda Granite|69591|5|Briefly described|p83|Mesoproterozoic|Mesoproterozoic|Westernmost Georgetown Inlier.||Esmeralda Supersuite.|||Fe-rich granite; contains fayalite.|
24432|Nonda Granite|73527|6|Mentioned|p2|||Georgetown Inlier, western domain.||Esmeralda Supersuite, western part||||
24432|Nonda Granite|75079|6|Mentioned|p6, 10-12|Mesoproterozoic|Mesoproterozoic|Northeast Queensland. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|1550 Ma.|Esmeralda Supersuite.||||
80901|Normanton Granite|69593|5|Briefly described|p512|||Jardine Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|328 Ma.||||I-type.|
41141|North Arm Volcanic Group|50320|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||28-MAY-04
41141|North Arm Volcanic Group|65452|5|Briefly described|p2-4, p35|Late Triassic|Late Triassic|Appears as North Arm Volcanics on p35. Occupies Yandina Creek Caldera. Mafic to intermediate volcanism followed by significant periods of voluminous silicic magmatism and development of large caldera system.|217 +/- 2 Ma; 213 +/- 6 Ma (K-Ar).||||Lower sequence: andesitic lavas and debris flows. Middle sequence: rhyolitic ignimbrites and bedded tuffs associated with caldera collapse. Upper sequence: rhyolitic lavas and bedded tuffs.|
41141|North Arm Volcanic Group|67203|6|Mentioned|p3, p36-37|Triassic|Triassic|Further geochronological work is required to determine the distribution (especially the width) of the Late Triassic volcanic belt.||||||
41141|North Arm Volcanic Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga Volcanic Group; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
41141|North Arm Volcanic Group|68679|4|Described|p326, p328-329, p387, p429, p434-436|Late Triassic|Late Triassic|See also p469, p472. North D'Aguilar Subprovince, northern New England Orogen. Described in some detail. Is divided into 18 subunits or members. Hosts extensive hydrothermal alteration systems and epithermal mineralisation. Contains Late Triassic plants.|217 +/- 2 Ma (K-Ar: Ashley and Shaw, 1993).||Wappa, Ninderry, Kenilworth Bluff, Carol Creek, Yandina Creek, Dunethin, Kilcunda, Eumundi, Perwillowen Rhyolites; Valdora Dacite; Kullangor Formation.|Unconformably overlies Amamoor and Cambroon beds, Gobongo Metamorphics and Mount Mia Serpentinite. Is intruded by Eerwah Vale Tonalite.|Undifferentiated: andesite and rhyolite, epiclastic sediments. A lower interval of andesitic lavas and pyroclastic deposits, overlain by more felsic, rhyolitic to dacitic ignimbrite, air fall tuff and lava flows.|
41141|North Arm Volcanic Group|69594|5|Briefly described|p519, p546-547, p561, p572|Late Triassic|Late Triassic|Southern Nambour Basin. Source of detritus for Nambour Formation.||||Is overlain by Nambour Formation.||
41141|North Arm Volcanic Group|69952|5|Briefly described|p2 Tb.i, p47-50|Late Triassic|Late Triassic|SHRIMP U-Pb zircon magmatic crystallisation age. Previous Ar-Ar and K-Ar age determinations ranged from c.235 Ma to c.224 Ma (Little et al., 1993; Sliwa, 1994). Dated sample (2123254/DPMR385) is from one of several bodies of intermediate to felsic volcanics that crop out more than 40 km northwest of the main body.|229.0 +/- 1.7 Ma (Cross et al., 2015).||Includes Wappa Rhyolite.||Includes a flow-banded dacitic unit.|30-NOV-15
41141|North Arm Volcanic Group|71592|5|Briefly described|Appendix A.|||New England Orogen.|229+/-1.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dacite.|
41141|North Arm Volcanic Group|73450|6|Mentioned|p84, p87|Triassic|Triassic|||||||
29620|North Brigooda Suite|43005|5|Briefly described|p217|||This is a xenolith suite within the Boyne Basalt field. Related to Brigooda Basalt?||||||21-MAR-23
36607|North Edge Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 387.  S-Type.||||||
70396|North Gwynne Granite|65452|6|Mentioned|p6 Fig.2, p29|Late Triassic|Late Triassic|Geochemistry briefly described.||||||
70396|North Gwynne Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pale pink to red, coarse to very coarse-grained biotite granite; medium grained porphyritic biotite monzogranite.|
70396|North Gwynne Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pale pink to red, coarse to very coarse-grained biotite granite; medium-grained porphyritic biotite monzogranite.|
70396|North Gwynne Granite|68679|5|Briefly described|p428, p432|Late Triassic|Late Triassic|Northern New England Orogen; Agnes Waters area.|||||Pale pink to red, coarse- to very coarse-grained biotite granite; medium-grained porphyritic biotite monzogranite.|
70396|North Gwynne Granite|72297|6|Mentioned|p758|||Near Lowmead, amethyst and quartz crystals commonly with colour zoning occur in decomposed granite.||||||
70396|North Gwynne Granite|73450|6|Mentioned|p16|||||||||
75153|North Island granite|60425|4|Described|p98, p100, p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name for granite on North Island (Bedarra Granite Belt). Age:335+/-6Ma (SHRIMP). Pale grey-pale brown(altered), med.-gr., slightly porphyritic biotite granite; + sparse feldspar phenocrysts up to ~1.5cm long. Forms dykes that cut Brook granite||||||07-FEB-11
36728|Northedge Granite|23423|5|Briefly described|p246|||Originally assigned to the Mount Alto Supersuite. Of Whypalla Supersuite.||||||
36728|Northedge Granite|50387|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Kennedy Province. Age: 277 Ma (K-Ar). Of Whypalla Supersuite||||||11-JUN-04
36728|Northedge Granite|60425|4|Described|p82, p274-5 Appdx. 1|Early Permian|Early Permian|Of Curraghmore Suite (Whypalla Supersuite). Formerly included in Mount Alto Supersuite. Age: 289-277Ma (Rb-Sr). S-type. Mod'ly to highly porphyritic (garnet-) tourmaline-muscovite-biotite granite with scarce enclaves -- further lithol. details (p275.).||||||07-FEB-11
36728|Northedge Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Curraghmore Suite.||||
22568|Northumberland Serpentinite|23330|6|Mentioned|1077||Permian|||||||
22568|Northumberland Serpentinite|43754|4|Described|p574|||||||||
22568|Northumberland Serpentinite|63600|4|Described|p900, p901-902|||Forms most of the South Island of the Percy Isles. Comprises serpentinised peridote in which chromite grains are the only relict magmatic minerals, with dykes and elongate inclusions of altered gabbro and dolerite. See also p914.||||||07-FEB-11
22568|Northumberland Serpentinite|68008|6|Mentioned|p488|||South Island, Percy Isles. The mantle component of a supra-subduction zone ophiolite; reacted with boninitic liquids.||||||
22568|Northumberland Serpentinite|71702|5|Briefly described|p177-178, p176 Fig. 2, p183,184,185,186|Permian||South Percy Island, Percy Isles.  ~100km NE of Marlborough Terrane. Age > 271.6 +/- 3.5 Ma, from dated cross-cutting dyke (PE1519a)||||Cut by unnamed dacitic dyke, syenite dyke.|Weakly foliated basaltic lava and intercalated  sedimentary rocks that have been metamorphosed at greenschist facies.|
38883|Norton Tonalite|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
38883|Norton Tonalite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgno].  Pale grey medium-grained lecucratic hornblende-biotite tonalite.||||||
38883|Norton Tonalite|68008|4|Described|p329, p334-335, p416-418, p486|Triassic|Permian|New unit, named after the Norton goldfield and Norton Creek. Previously mapped as an isolated intrusion of Miriam Vale Granodiorite. 35km SSE of Calliope. Forms low hills. Geophysics briefly described. Geochemistry described. Not dated. Hosts numerous gold-bearing reefs of the Norton goldfield.||||Intrudes the Miriam Vale Granodiorite, Wandilla Formation and Castletower Granite.|A very uniform, grey, medium-grained, leucocratic hornblende-biotite tonalite.|
38883|Norton Tonalite|68679|5|Briefly described|p421, p427|||Gayndah-Gladstone belt. Geochemistry briefly described.|||||Leucocratic hornblende-biotite tonalite.|
22569|Nostone Creek Granodiorite|22675|4|Described|p113|Early Permian|Early Permian|||||||
22569|Nostone Creek Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 237. I-Type.||||||
22569|Nostone Creek Granodiorite|43259|4|Described|Appendix 1,p32.||Early Permian|U-Pb zircon age is 289+/-4 Ma.||||||
22569|Nostone Creek Granodiorite|43391|5|Briefly described|Map legend|Early Permian|Early Permian|Fine to medium hornblende-biotite granodiorite.||||||23-JUN-04
22569|Nostone Creek Granodiorite|43734|6|Mentioned|p6|||U-Pb age: 289.3+/-5.9 Ma||||||
22569|Nostone Creek Granodiorite|60659|5|Briefly described|p18|||Grey to slightly pinkish hornblende-biotite granodiorite that grades to quartz monzodiorite.  Intrudes Earlscliffe Dacite.||||||07-FEB-11
22569|Nostone Creek Granodiorite|68901|5|Briefly described|p5, p121-p124, p145|Early Permian|Early Permian|Kennedy Igneous Association, Thomson Region. Appears as Nostone Granodiorite on p145. Forms prominent outcrops in the Ten Mile Creek. Informally referred to as the Black Hole granite. SHRIMP age is interpreted as the age of magmatic crystallisation. Older age determination: 289.3+/-5.9 Ma (of Black, in Oversby & others, 1994) also mentioned.|292.6 +/- 2.2 (SHRIMP U-Pb)|||Adjacent to Earlscliff Dacite.|Pale pinkish grey, fine- to medium-grained, moderately porphyritic biotite-hornblende quartz monzodiorite.|16-NOV-18
22569|Nostone Creek Granodiorite|69593|5|Briefly described|p495, p513|Permian|Late Carboniferous|Burdekin Falls Subprovince. Sm-Nd isotope data tabulated.|293 +/- 2 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
22569|Nostone Creek Granodiorite|70740|5|Briefly described|p8, p120, p123, p127|Sakmarian|Sakmarian|SHRIMP age derived from Black (1994). An additional SHRIMP age from Cross et al, 2012 is provided on p8. |289.3 +/- 5.9 (SHRIMP U-Pb)||||Fine to medium-grained hornblende-biotite granodiorite to quartz monzodiorite.|
22569|Nostone Creek Granodiorite|71592|5|Briefly described|Appendix A.|||Drummond Basin.|289+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
32127|Nulambie Granite|23037|5|Briefly described|p77|Triassic|Silesian|||||||
32127|Nulambie Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgnl].  Grey, medium-grained, altered biotite and honrblende biotite granite to granodiorite.||||||
32127|Nulambie Granite|50273|5|Briefly described|Map legend|Early Triassic|Late Permian| Grey, medium-grained, altered, biotite and hornblende-biotite granite to granodiorite.||||||
32127|Nulambie Granite|65388|3|Fully described|p328-329,  p237, 238,  p301|Early Triassic|Late Permian|Intrudes rocks assigned to Camboon Volcanics, but they could be Torsdale Volcanics. Age uncertain. Could be older. Mainly light grey, medium grained to slightly porphyritic biotite-hornblende quartz monzonite and granite to granodiorite.||||||
32127|Nulambie Granite|68679|5|Briefly described|p419|||A ~3 km2 pluton, west of the main Rawbelle Batholith. Age uncertain.||||Intrudes Camboon Volcanics.|Altered, biotite and hornblende-biotite granite to granodiorite.|
30012|Nulbullulul Granite|23422|5|Briefly described|Plate 7.3|Late Permian|Late Permian|||||||
30012|Nulbullulul Granite|23423|5|Briefly described|p311 Table 7.4||Late Permian|Age: 261 +/- 3 Ma. Also see p251. Pieter Botte Supersuite.||||||
30012|Nulbullulul Granite|23430|5|Briefly described|p490|||Kennedy Province.||||||
30012|Nulbullulul Granite|43070|2|Defined|p82|||||||||
30012|Nulbullulul Granite|43285|5|Briefly described|Map Legend||Late Permian|||||||
30012|Nulbullulul Granite|43625|5|Briefly described|p35,52,128,Apend.8|||Age: 261+/-3 Ma Shrimp. Permian||||||
30012|Nulbullulul Granite|60425|5|Briefly described|p51 Tb. 3, p54 Tb. 4, p272-3 Appdx. 1|Late Permian|Late Permian|Of Nulbullul Suite (Peiter Botte Supersuite). Age: 261+/-3Ma (SHRIMP). Intruded Hodgkinson Fm+Obree Point Volcs. I-type, hornblende-biotite granite, fine to med. Gr., slightly to mod'ly porphyritic, sparse tourmaline-quartz aggregates - more lith.detail.||||||07-FEB-11
30012|Nulbullulul Granite|69592|6|Mentioned|p249 Fig.4.34|Permian|Permian|Time-space diagram of Kennedy Igneous Association granitoids relative to Permian deformation in the Palmer-Barron Subprovince.||||||
30012|Nulbullulul Granite|69593|5|Briefly described|p480, p483|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |261 +/- 3 Ma (SHRIMP U-Pb zircon).|Nulbullulul Suite.||||
30012|Nulbullulul Granite|72983|6|Mentioned|p4|Wuchiapingian|Capitanian||261 +/- 3 Ma||||I-type granites.|
69319|Nulbullulul Suite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Yates Supersuite. Includes Nulbullul, Thornton and Bunk Creek Granites. I-type.||||||07-FEB-11
69319|Nulbullulul Suite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |261 +/- 3 Ma (SHRIMP U-Pb zircon).||Nulbullulul, Thornton, Bunk Creek Granites.|||
77820|Nulla Basalt Group|68553|6|Mentioned|Map legend|Quaternary|Neogene|Parts of both this unit and the McBride Basalt Group; the Atherton, Chudleigh, McIvor River, McLean, Piebald, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn. Parts of this unit, as well as the Barkers and Yates Creek Basalts; the Maer Volcanics; parts of the McBride Basalt Group, and unnamed basalt flows, are all mapped under the symbol, Qbn.||||||
77820|Nulla Basalt Group|73115|6|Mentioned|[See comments]|Holocene|Pliocene|Nulla Basalt Province. Grouped into Quaternary, Quaternary-Pliocene, and Pliocene on maps. p: 76-77, 90, 94, 99, 105, 110, 112, 115, 119-120.|0-5.33 Ma|||||
37838|Nundah suite|23291|5|Briefly described|p35|||Informal name. Geological Province: Georgetown Region.||||||08-JUL-15
76903|Nundata Granite|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Doherty-Fig Tree Gully Domain, Mount Isa Inlier. Williams Igneous Event.|1527 +/- 4 Ma.|Williams Supersuite.|||Medium- to coarse-grained highly altered pink granite, locally strongly foliated to mylonitic.|
76903|Nundata Granite|69056|6|Mentioned|Time-Space plot sheet|Calymmian|Calymmian||1527 +/- 4 Ma.|||||
76903|Nundata Granite|69591|5|Briefly described|p59|||Maramungee area.||Williams Supersuite.|||Medium- to coarse-grained highly altered pink granite, locally strongly foliated to mylonitic.|
76903|Nundata Granite|70353|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium- to coarse-grained highly altered pink granite, locally strongly foliated to mylonitic.|
76903|Nundata Granite|70354|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium- to coarse-grained highly altered pink granite, locally strongly foliated to mylonitic.|
76903|Nundata Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite|||Medium to coarse-grained highly altered pink granite, locally strongly foliated to mylonitic. Hornblende diorite (mapped separately).|05-MAY-16
76903|Nundata Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes an unnamed hornblende diorite.||Williams Supersuite.|Includes one unnamed member.||Medium-coarse grained highly altered granite, locally strongly foliated to mylonitic.|
77679|Nursery Creek Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. High K, Th and U radiometric responses.||Unit in O'Briens Creek Supersuite.|||Pale pink, fine- to medium-grained, moderately porphyritic, leucocratic muscovite-biotite granite, variably altered; similar biotite monzogranite, with quartz phenocrysts commonly pale to dark grey.|
36981|Nutgrove Rhyolite Member|23799|3|Fully described|p56, p9 Tb. 1|Tertiary|Tertiary|Supersedes Nutgrove Agglomerate Member in this publication.  Of the Main Range Volcanics. Rhyolite breccia.  Unconformably overlies the Marburg Formation.  Geological Province: Main Range-Lamington Volcanic Province.||||||
36981|Nutgrove Rhyolite Member|23800|5|Briefly described|Map Legend|Pliocene|Miocene|Of Main Range Volcanics.||||||
36981|Nutgrove Rhyolite Member|50384|5|Briefly described|Map Legend|Tertiary|Tertiary|Of Main Range Volcanics.||||||
36981|Nutgrove Rhyolite Member|73450|4|Described|p90-91|||Northern Main Range. Previously called Nutgrove Agglomerate Member. Locally divided into subunits.||Main Range Volcanics|||Cobble to boulder agglomerate with phenoclasts of granite and basalt in a white, fine-grained matrix as well as minor rhyolite intrusives, breccias, flows, and tuff with tuffaceous sandstone at the top.|
27864|Nychum Volcanics|23420|5|Briefly described|p 131|||Previously included the rocks of the Mitchell River Volcanics||||||
27864|Nychum Volcanics|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
27864|Nychum Volcanics|23423|3|Fully described|p304 Table 7.3||Early Permian|Age:  277 +/- 4 Ma (U-Pb, zircon, SHRIMP). Also see p235. Underlain by Hodgkinson and Chillagoe Formations, Wotan Granodiorite, Nightflower Dacite (unconformable). Kennedy Igneous Province.||||||22-APR-09
27864|Nychum Volcanics|23430|5|Briefly described|p475|||||||||
27864|Nychum Volcanics|23496|5|Briefly described|p47|||||||||
27864|Nychum Volcanics|23497|6|Mentioned|p32||Permian|||||||
27864|Nychum Volcanics|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V119. I-Type.||||||
27864|Nychum Volcanics|23616|6|Mentioned|Table 3 p46|||||||||
27864|Nychum Volcanics|23713|3|Fully described|p17-20||Early Permian|Maximum thickness: 250 m.||||||
27864|Nychum Volcanics|24013|5|Briefly described|p18 Tb. 1|Early Triassic|Permian|Correlated with Agate Creek Volcanics.||||||
27864|Nychum Volcanics|24086|5|Briefly described|p312 Fig. 1|Early Permian|Early Permian|||||||
27864|Nychum Volcanics|24485|6|Mentioned|p40|||||||||
27864|Nychum Volcanics|29605|6|Mentioned|p1|||||||||
27864|Nychum Volcanics|29632|6|Mentioned|p103|||||||||
27864|Nychum Volcanics|29793|4|Described|p189|||||||||
27864|Nychum Volcanics|29794|6|Mentioned|P.1168|||||||||
27864|Nychum Volcanics|29796|6|Mentioned|Fig.1|||||||||
27864|Nychum Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27864|Nychum Volcanics|31168|5|Briefly described|p10|||||||||
27864|Nychum Volcanics|31832|6|Mentioned|Table 6|||||||||
27864|Nychum Volcanics|33528|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27864|Nychum Volcanics|33880|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27864|Nychum Volcanics|34046|6|Mentioned|Table II|||||||||
27864|Nychum Volcanics|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
27864|Nychum Volcanics|34998|6|Mentioned|p347|||||||||
27864|Nychum Volcanics|36527|6|Mentioned|p162|||||||||
27864|Nychum Volcanics|36794|6|Mentioned|p386|||||||||
27864|Nychum Volcanics|37400|6|Mentioned|p312|||||||||
27864|Nychum Volcanics|37575|4|Described|p179|||||||||
27864|Nychum Volcanics|37613|6|Mentioned|p247|||See also Fig.1||||||
27864|Nychum Volcanics|38225|4|Described|p375|||See also Fig.2.||||||
27864|Nychum Volcanics|39252|6|Mentioned|p11|||Refs White (1965); Black.et.al (1972), Balme (1973)||||||
27864|Nychum Volcanics|39261|6|Mentioned|Fig. 9|||||||||
27864|Nychum Volcanics|39266|5|Briefly described|Table 1|||||||||
27864|Nychum Volcanics|39445|5|Briefly described|Table 7|||See also Table 8||||||
27864|Nychum Volcanics|39564|6|Mentioned|Table 2|||||||||
27864|Nychum Volcanics|39689|6|Mentioned|p59|||||||||
27864|Nychum Volcanics|40623|5|Briefly described|p88|||||||||
27864|Nychum Volcanics|40892|5|Briefly described|p75|||||||||
27864|Nychum Volcanics|42200|6|Mentioned|Fig.1 P325|||||||||
27864|Nychum Volcanics|42547|5|Briefly described|p74|||||||||
27864|Nychum Volcanics|42681|6|Mentioned|p19|||||||||
27864|Nychum Volcanics|42798|6|Mentioned|p57|||||||||
27864|Nychum Volcanics|43013|5|Briefly described|p241|||||||||
27864|Nychum Volcanics|43018|6|Mentioned|p390|||||||||
27864|Nychum Volcanics|43060|5|Briefly described|p116|||||||||
27864|Nychum Volcanics|43083|4|Described|p79||Early Permian|Dominated by rhyolite lava flows and associated felsic airfall pyroclastic deposits.||||||17-JUN-09
27864|Nychum Volcanics|43087|5|Briefly described|Fig.6|||||||||
27864|Nychum Volcanics|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Grey aphyric to sparsely porphyritic rhyolite; black obsidian; rhyolite breccia; andesite and basalt; rhyolitic tuff, conglomerate.||||||15-JUN-06
27864|Nychum Volcanics|43254|5|Briefly described|map legend||Early Permian|||||||
27864|Nychum Volcanics|43259|4|Described|Appendix 1,p12.||Early Permian|Rb-Sr age is 270+/-16 Ma.||||||
27864|Nychum Volcanics|43285|5|Briefly described|Map Legend||Early Permian|||||||
27864|Nychum Volcanics|43625|3|Fully described|p38|||||||||
27864|Nychum Volcanics|43626|4|Described|p93|Early Permian|Late Carboniferous|||||||
27864|Nychum Volcanics|43896|14|Not recorded|Map Legend||Late Permian|||||||
27864|Nychum Volcanics|43898|14|Not recorded|Map Legend||Late Permian|||||||
27864|Nychum Volcanics|43899|14|Not recorded|p274,276||Permian|||||||
27864|Nychum Volcanics|43974|14|Not recorded|p505|||||||||
27864|Nychum Volcanics|44025|14|Not recorded|p353||Permian|||||||
27864|Nychum Volcanics|44258|14|Not recorded|p2,17,18||Late Paleozoic|Includes different aged masses.||||||07-NOV-08
27864|Nychum Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
27864|Nychum Volcanics|44425|14|Not recorded|p14,15,17-22,opp.11,|||Map. Fossils.||||||
27864|Nychum Volcanics|44843|14|Not recorded|p179|||||||||
27864|Nychum Volcanics|45008|14|Not recorded|p12,17,29,32,36-7||Late Permian|||||||
27864|Nychum Volcanics|45014|2|Defined|p61,106-109,111-117,||Early Carboniferous|p157,Pl.38,Tb.1. (Middle Carboniferous)||||||
27864|Nychum Volcanics|45025|2|Defined|p60-1,71,anal.p73||Late Permian|||||||
27864|Nychum Volcanics|45076|3|Fully described|p106|||See also p37, p40. Upper Carboniferous.||||||22-APR-09
27864|Nychum Volcanics|45087|5|Briefly described|p97|||Chemical analyses||||||
27864|Nychum Volcanics|45113|6|Mentioned|p43|||||||||
27864|Nychum Volcanics|46845|6|Mentioned|Table 1|||||||||
27864|Nychum Volcanics|48976|6|Mentioned|p7|||||||||
27864|Nychum Volcanics|60087|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Rhyolite, welded tuff, andesite, basalt, arkose, shale, coaly shale, limestone.||||||
27864|Nychum Volcanics|60425|3|Fully described|p44 Tb. 3, p67-70, p108|Early Permian|Early Permian|Includes 30 informal subunits. Unconformable on Hodgkinson and Chillagoe Fms, Wotan Granodiorite, Nightflower Dacite + Wakara Subgroup lavas. A-type. Age: 277+/-4Ma.Thickness: ~250m. Lithological details+detailed interpretation of origin and age included||||||07-FEB-11
27864|Nychum Volcanics|62523|6|Mentioned|p9|||Formerly noted by Ball (1912) as coarsely fragmented rocks representing an extrusive vent but subsequently assigned to Nychum Volcanics (Branch 1966; deKeyser and Lucas 1968). Here, tentatively assigned to Featherbed Volcanic Gp as Breccia Creek Rhyolite.||||||07-FEB-11
27864|Nychum Volcanics|65114|5|Briefly described|p383 Tb.1, p398|Cisuralian|Upper Carboniferous|300-280 Ma (?start at 313 Ma); Tectonic unit: Kennedy Igneous Province; zircons from a rhyolite SHRIMP dated at 277 +/- 4 Ma||||||
27864|Nychum Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek, Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork and Mitchell River Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
27864|Nychum Volcanics|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|278 +/- 3 Ma (SHRIMP).|||||
27864|Nychum Volcanics|69593|5|Briefly described|p483, p485-486, p504, p510|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Early Permian.|277 Ma.||||A-type.|
27864|Nychum Volcanics|72297|5|Briefly described|p732|Permian|Permian|Kennedy Igneous Association. At the Nychum (Wrotham) deposit, 50km NW of Chillagoe, perlite occurring as discrete layers in the unit is mined.||||||
27864|Nychum Volcanics|72983|6|Mentioned|p19|Roadian|Kungurian|Suspected coeval with Collins Weir Rhyolite, Tinaroo Granite, Hope Vale Granite and Featherbed Volcanic Group.|277 +/- 4 Ma|||||
69350|Nymbool Suite|60425|5|Briefly described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of the Ootann Supersuite. Contains the Nymbool Granite. I-type. Age: ~316Ma, 318+/-43Ma (Rb-Sr).||||||07-FEB-11
36486|O'Briens Creek Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 63.  I-Type.||||||
36486|O'Briens Creek Microgranite|69593|5|Briefly described|p487 Fig.6.9|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.||Intrudes Elizabeth Creek Granite.||
69337|O'Briens Creek Suite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||O'Briens Creek Supersuite.|O'Briens Creek Microgranite.||I-type.|
29322|O'Briens Creek Supersuite|23085|5|Briefly described|p670||Carboniferous|||||||
29322|O'Briens Creek Supersuite|23291|4|Described|44, p96 Tb. 3.11, p100 Tb. 3.12|Late Carboniferous|Carboniferous|Geological Province: Tata Batholith. Most granites of the O'Briens Creek Supersuite were originally mapped as "Elizabeth Creek Granite" (de Keyser & Wolff 1964; White 1965; Branch 1966; de Keyser & Lucas 1968).||||||08-JUL-15
29322|O'Briens Creek Supersuite|23423|4|Described|p315 Table 7.4||Late Carboniferous|Age: ~300-315 Ma (Rb-Sr). Also see p241-242.||||||
29322|O'Briens Creek Supersuite|23430|5|Briefly described|p495|||Kennedy Province||||||
29322|O'Briens Creek Supersuite|23431|5|Briefly described|p539|||||||||
29322|O'Briens Creek Supersuite|23497|6|Mentioned|p32|||Intrude lower part of Glen Gordon Volcanics.||||||
29322|O'Briens Creek Supersuite|23500|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||||||
29322|O'Briens Creek Supersuite|23501|6|Mentioned|map legend|Late Carboniferous|Late Carboniferous|||||||
29322|O'Briens Creek Supersuite|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
29322|O'Briens Creek Supersuite|23503|5|Briefly described|Map Legend|||||||||
29322|O'Briens Creek Supersuite|23506|5|Briefly described|Map Legend||Late Carboniferous|||||||
29322|O'Briens Creek Supersuite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
29322|O'Briens Creek Supersuite|23549|5|Briefly described|p527|||Interdigitates with the Ootann Supersuite.  See also p516 Fig. 1.||||||05-APR-05
29322|O'Briens Creek Supersuite|23616|4|Described|p75-77||Carboniferous|Isotopic ages ~310 Ma-315 Ma. Rb-Sr ~309-315 Ma. Rb-Sr biotite ~321 Ma. I-type Granites. Dargalong Province.||||||
29322|O'Briens Creek Supersuite|23617|5|Briefly described|p15|||||||||
29322|O'Briens Creek Supersuite|23624|5|Briefly described|p20|||||||||
29322|O'Briens Creek Supersuite|24485|6|Mentioned|p50 Tb.8|||||||||
29322|O'Briens Creek Supersuite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
29322|O'Briens Creek Supersuite|24579|6|Mentioned|p799|Late Carboniferous|Carboniferous|||||||
29322|O'Briens Creek Supersuite|43060|4|Described|p101|||||||||
29322|O'Briens Creek Supersuite|43083|4|Described|p125|||Includes McCord Granite. Comprises highly fractionated granite and subordinate leucoadamellite.||||||07-APR-15
29322|O'Briens Creek Supersuite|43087|6|Mentioned|p24|||||||||
29322|O'Briens Creek Supersuite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Includes the Herberton and Nettle Suites.||||||15-JUN-06
29322|O'Briens Creek Supersuite|60425|3|Fully described|p53, p60 Tb. 4, p72-73, p282-3 Appdx. |Early Permian|Late Carboniferous|Comprises numerous named/unnamed subunits.Intruded lower part of Glen Gordon Volcanics (ATHERTON). Cut by Ootann Supersuite granites. Age range: 315-300Ma (Rb-Sr istotopic). Very detailed lithology included for these I-type biotite granites/microgranites||||||07-FEB-11
29322|O'Briens Creek Supersuite|61784|5|Briefly described|p297|||Of Mount Surprise-Herberton Group.||||||
29322|O'Briens Creek Supersuite|62371|5|Briefly described|p472 Fig.3|Carboniferous|Carboniferous|Shows gold mineralisation.||||||
29322|O'Briens Creek Supersuite|63140|6|Mentioned|p572 fig 3|Carboniferous|Carboniferous|||||||
29322|O'Briens Creek Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Carboniferous|Geological province: Hodgkinson Province. Gold mineralisation.||||||
29322|O'Briens Creek Supersuite|65455|6|Mentioned|p7, p8 Fig. 4|Permian|Carboniferous|Prominent representatives of high-U igneous rocks in the Georgetown-Cairns-Charters Towers region.||||||09-MAY-12
29322|O'Briens Creek Supersuite|66529|5|Briefly described|p77 |Late Carboniferous|Late Carboniferous|Has highest Hot Rock heat production values.|||||Felsic intrusives.|
29322|O'Briens Creek Supersuite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Emuford and Sundown Granites.|||
29322|O'Briens Creek Supersuite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Emuford and Sundown Granites.|||
29322|O'Briens Creek Supersuite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes McCord, Madjack, Emuford, Opah, Billings, Nursery Creek and Atlanta Granites.|||
29322|O'Briens Creek Supersuite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Late Carboniferous age. Also includes Kangaroo Rat Granite, Desert Creek Granite, Flynns Creek Granite, McCord Granite, First Bull Run Granite, Elizabeth Creek Granite, Angore Granite.|||Includes Butters Creek Granite, Charlies Knob Granite, Pat and Peter Creek Granite, Fulford Creek Granite, Burlington Creek Granite, Rose Creek Granite, Wireyard Granite, Square Rock Granite.|Older than Brodies Camp Supersuite rocks. Younger than White Springs Supersuite rocks.||
29322|O'Briens Creek Supersuite|68553|6|Mentioned|Map legend|Permian|Carboniferous|This unit (in part), as well as the Claret Creek, Glenmore, Ingham (in part), Almaden, Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk. It is also mapped (in part), as CPgk, with the Badu Suite and parts of the Almaden, Leichhardt, Ingham and Ootann Supersuites, and various ungrouped Carboniferous-Early Permian plutonic units. ||||||
29322|O'Briens Creek Supersuite|68576|5|Briefly described|Q_11: p18|Carboniferous|Carboniferous|28 km N of Ravenshoe. Hosts the Hypipamee Crater, thought to have resulted from a phreatic eruption.||||||
29322|O'Briens Creek Supersuite|69593|3|Fully described|p483, p485-486, p487 Fig.6.9, p489|||See also p502-504, p506, p508-509. Herberton Subprovince, Kennedy Igneous Association. Highly mineralised in Sn and/or W. Comprises over 80 identified, mostly unnamed, usually large putons that crop out over ~2500 km2 concentrated on both sides of the Palmerville Fault. Most chemically evolved I-type magmatism within the Kennedy Igneous Association. Contains most of the fluorite-bearing leucogranites in the Province. Geochemistry detailed.|~322-318 Ma.||Cherry Creek, Go Sam, Nettle, O'Briens Creek Suites; Elizabeth Creek, Burlington, Emuford, Koogangoona, Herberton Hill Granites.||Porphyritic to seriate to equigranular pink/red biotite leucogranite and microgranite; common pegmatite and miarolitic cavities; wide variety of accessory phases (eg zircon, ilmenite, monazite, thorite, topaz, common fluorite). Strongly fractionated.|
28021|O'Lane Formation|23420|5|Briefly described|p 142 table 4.4|||In the Edward River Metamorphic Group. Thickness 800m||||||
28021|O'Lane Formation|43596|4|Described|p16, p20 Tb. 1||Proterozoic|Of the Edward River Metamorphic Group. Conformably overlies Drovers Lagoon Formation; conformably overlain by Crosbie Formation. Max. thickness: 800m. Comprises fine- to medium-grained, light grey, muscovite schist commonly interbedded with quartzite.||||||27-JAN-09
28021|O'Lane Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Edward River Metamorphic Group||||||24-JAN-05
28021|O'Lane Formation|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. 800m thick.||Edward River Metamorphic Group.||Partly correlates with Astrea Formation.|Muscovite schist-phyllite and slate, quartzite and metasandstone.|
30082|OK Member|23086|6|Mentioned|p668|||Hodgkinson Formation?||||||
30082|OK Member|23423|5|Briefly described|p232|||Hodgkinson Formation; Hodgkinson Province.||||||
30082|OK Member|23713|4|Described|p15||Late Devonian|Previously mapped as eastern part of the Mount Garnet Formation. Age based on examination of the radiolarians. Of Hodgkinson Formation. Hodgkinson Province.||||||
30082|OK Member|43083|3|Fully described|p53 Tb 5, p66||Late Devonian|Of the Hodgkinson Formation. Formerly mapped as the estern part of Mount Garnet Formation. Geological province: Hodgkinson Province.||||||17-JUN-09
30082|OK Member|43254|5|Briefly described|map legend|Late Devonian|Late Silurian|Of the  Hodgkinson Formation.||||||21-APR-09
30082|OK Member|43285|5|Briefly described|Map Legend|||age Late Silurian? to Late Devonian?Of Hodgkinson Formation.||||||
30082|OK Member|43625|4|Described|p19,26,30|||||||||
30082|OK Member|60357|5|Briefly described|Map Legend|Late Devonian|Late Silurian|Geological Province: Hodgkinson Province. Of the Hodgkinson Formation.||||||
30082|OK Member|60425|4|Described|p16 Tb. 1, p27|||Of the Hodgkinson Formation. Previously mapped as eastern part of Mount Garnet Formation - metabasalts, characterised by numerous closely spaced chert lenses. Geological province: Hodgkinson Province.||||||07-FEB-11
30082|OK Member|69030|5|Briefly described|p6|Devonian|Devonian|Chillagoe Subprovince, Hodgkinson Province.||Hodgkinson Formation.||||
30082|OK Member|69592|5|Briefly described|p231 Fig.4.4, p232, p237|Devonian|Silurian|Mossman Orogen, Palmer-Barron Subprovince, Hodgkinson Province. Regarded more as sedimentary and volcanic rock assemblages rather than stratigraphic units which imply superpositional relationships. Forms a narrow, elongate, fault-bounded, chert-dominated belt on the eastern margin of the Kitoba Member.||Hodgkinson Formation.||||
30082|OK Member|70345|4|Described|p13, p22-27|Devonian|Devonian|Forms a narrow, chert-dominated belt on the eastern margin of the Kitoba Member. Hosts radiolaria with three-bladed spines. Sample locality, zircon morphology, SHRIMP analyses and results are discussed. On the basis of an early Frasnian max dep age and late Devonian this member may represent a fault-bounded ""out-of-sequence' assemblage.||Hodgkinson Formation||Faulted against the Kitoba Member.|Sandstone interlayered with strongly cleaved, mainly thin-bedded siltstone and dark grey mudstone.|
34118|Oak Vale Suite|22630|6|Mentioned|p 3|||||||||
34118|Oak Vale Suite|22844|6|Mentioned|p46|||||||||
34118|Oak Vale Suite|23422|4|Described|p174, p211 Table 6.7|Ordovician|Ordovician|Part of Fat Hen Creek Complex?||||||
36621|Oak Vale granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 469.  I-Type.||||||
26817|Oakdale Sandstone|23799|3|Fully described|p53, p10 Tb. 1|Early Eocene|Early Eocene|Overlain by Main Range Volcanics; unconformably overlies Wooroonden Granodiorite.  Max. thickness: <100m.  Geological Province: Main Range-Lamington Volcanic Province.||||||
26817|Oakdale Sandstone|23800|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
26817|Oakdale Sandstone|35101|3|Fully described|p56|||||||||
26817|Oakdale Sandstone|36926|6|Mentioned|p165|||See also P175.||||||
26817|Oakdale Sandstone|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26817|Oakdale Sandstone|37376|6|Mentioned|p491|||||||||
26817|Oakdale Sandstone|38371|6|Mentioned|p666|||||||||
26817|Oakdale Sandstone|38373|6|Mentioned|p624|||||||||
26817|Oakdale Sandstone|39445|5|Briefly described|Table 14|||||||||
26817|Oakdale Sandstone|40475|6|Mentioned|p9|||||||||
26817|Oakdale Sandstone|41917|6|Mentioned|p531|||||||||
26817|Oakdale Sandstone|44581|14|Not recorded|p351||Cenozoic|Overlies Kinbombi Boulder Beds. Overlain by rhyolites and basalts.||||||19-NOV-08
26817|Oakdale Sandstone|44760|14|Not recorded|p405,406||Tertiary|||||||
26817|Oakdale Sandstone|44923|5|Briefly described|Map Legend||Tertiary|||||||
26817|Oakdale Sandstone|50320|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
26817|Oakdale Sandstone|60077|5|Briefly described|Map legend|Tertiary|Tertiary|Sandstone, conglomerate, shale.||||||
26817|Oakdale Sandstone|60371|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, conglomerate, shale||||||02-SEP-04
26817|Oakdale Sandstone|61155|5|Briefly described|p19|Late Eocene||Overlies Pomona Beds? In the Brisbane region.||||||
26817|Oakdale Sandstone|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses Sandstone, and unnamed units, are all mapped under the symbol, Tl.||||||
26817|Oakdale Sandstone|69599|5|Briefly described|p580, p586, p596|Eocene|Eocene|Derrington (1954) and others. Near Murgon. 100m thick. At Boat Mountain, a mudstone interval contains a highly significant diverse Eocene vertebrate fossil assemblage (the Tingamarra Local Fauna), described and illustrated in detail on pp596-598. Capped by silcrete.|||||Poorly consolidated quartzose to sublabile lithic sandstone, conglomerate and mudstone; minor brown coal.|
29596|Oakview Metamorphics|22845|2|Defined|p54,65,79||Carboniferous|Previously mapped by Murphy 1976 as part of the Biggendon beds, possibly correlates with Rocksburg Greenstone.||||||
29596|Oakview Metamorphics|22846|6|Mentioned|p18||Carboniferous|||||||
29596|Oakview Metamorphics|23608|5|Briefly described|p56, p56 Table 1|||Recommended to be combined with Manumbar Metamorphic and called Manumbar Metamorphics due to their profound similarities.||||||
29596|Oakview Metamorphics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
29596|Oakview Metamorphics|44923|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36580|Oaky Creek granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 324.  I-Type.||||||
36580|Oaky Creek granite|60425|5|Briefly described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Informal name. Part of the Ootann Supersuite. I-type. Pink, fine- to coarse-grained biotite granite; minor biotite microgranite.||||||07-FEB-11
29981|Oaky Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
29981|Oaky Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 258. I-Type.||||||
29981|Oaky Granite|23616|6|Mentioned|Table 6 p73|||Of O'Briens Creek Supersuite.||||||
29981|Oaky Granite|43060|5|Briefly described|Table 6|||of O'Briens Creek Supersuite||||||
29981|Oaky Granite|43259|4|Described|Appendix 1,p34.||Carboniferous|||||||
29981|Oaky Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite but within the O'Briens Creek Supersuite. Includes No Hays Minas Granite on most recent maps. Pink to cream, fine-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
39609|Oasis Metamorphics|50200|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
39609|Oasis Metamorphics|50201|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
39609|Oasis Metamorphics|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|||||||07-NOV-08
39609|Oasis Metamorphics|61258|5|Briefly described|p387 Fig. 1|Paleoproterozoic|Neoproterozoic|Geological Province: Georgetown Inlier.||||||07-NOV-08
39609|Oasis Metamorphics|67455|4|Described|p573, pp575-577, pp580-583. |Early Paleozoic|Late Neoproterozoic|Western Greenvale Province. Forms basement. Metasedimentary and meta-igneous rocks derived from continental margin, shallow marine dolomitic and impure carbonates, shale and quartzofeldspathic sandstone, and mafic volcanic and/or intrusive tholeiitic rocks. Detrital zircon clusters at 1300 - 1250 Ma, 1200 - 1150 Ma and 540 - 520 Ma (U-Pb). Metamorphic rims aged 476 +/- 5 Ma (U-Pb zircon SHRIMP); ie Early Ordovician. Underlay extensional basin system and underwent extensional deformation.||||Intruded and metamorphosed by Lynwater Complex.|Lower unit of calc-silicate gneiss; middle unit of amphibolite with lesser biotite schists; upper unit of biotite gneiss with less common amphibole, calc-silicate gneiss and lenses of dolomitic marble; lenticular foliated granite masses throughout.|
39609|Oasis Metamorphics|68336|5|Briefly described|Map legend.|||Cape River Province. Age max: Neoproterozoic? Age min: Cambrian?|||||Biotite schist or gneiss, hornblende granofels or gneiss and minor amphibolite; some biotite orthogneiss (deformed granitoid).|11-MAY-15
39609|Oasis Metamorphics|68341|5|Briefly described|Map legend.|||Cape River Province. Age max: Neoproterozoic? Age min: Cambrian?|||||Biotite schist or gneiss, hornblende granofels or gneiss and minor amphibolite; some biotite orthogneiss (deformed granitoid).|11-MAY-15
39609|Oasis Metamorphics|68344|5|Briefly described|Map legend.||Neoproterozoic|Cape River Province. Eight facies are mapped separately. Age min: Early Paleozoic?|||||Calc-silicate gneiss; dolomitic marble with common tremolite; biotite and muscovite-biotite schist and amphibolite; amphibolite; biotite schist or gneiss, hornblende granofels or gneiss; banded-iron-formation; orthoamphibolite; serpentinite.|11-MAY-15
39609|Oasis Metamorphics|68346|5|Briefly described|Map legend.||Neoproterozoic|Age min: Early Paleozoic?|||||Calc-silicate (hornblende-diopside) gneiss; biotite and muscovite-biotite schist and amphibolite with pegmatite and leucogranite dykes; biotite schist or gneiss, hornblende granofels or gneiss and minor amphibolite.|11-MAY-15
39609|Oasis Metamorphics|68410|5|Briefly described|Map Legend|Paleozoic|Neoproterozoic|Early Paleozoic ? minimum age. Shown as older than the Delamerian Orogeny (ca. 500 Ma)and younger than D3 (c. 970 Ma?). Contains 3 unnamed subunits.|~ 970-500 Ma||||Biotite schist or gneiss, hornblende granofels or gneiss and minor amphibolite, some biotite orthogneiss; biotite and muscovite-biotite schist and amphibolite with abundant pegmatite and leucogranite dykes; calc-silicate (hornblende-diopside) gneiss.|
39609|Oasis Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Greenvale Province.||||||
39609|Oasis Metamorphics|68576|5|Briefly described|Q_11: p31-33|Cambrian|Neoproterozoic|Includes rocks to the E of the Lynd Mylonite Zone (=Tasman Line) which include late Neoproterozoic detrital zircons and metamorphic ovegrowths dated at ~480 Ma (cf. Einasleigh Metamorphics).|||||Strongly weathered gneiss, schist and amphibolite.|
39609|Oasis Metamorphics|68731|5|Briefly described|p151 Fig 3.51, p152, p159, p189|Cambrian|Furongian|Greenvale Province. Suggested that this unit is not part of the Einasleigh Metamorphics as originally thought by Withnall (1989) and Withnall et al. (1997). Minimum age constrained by the intrusive Lynwater Complex.|> 486 +/- 5 Ma; 477 +/- 6 Ma|||Intruded by the Lynwater Complex. Nonconformably overlain by the Conjuboy Formation.|Dominated by upper amphibolite grade gneiss and amphibolite: calc-silicate gneiss, amphibolite with minor biotite schist, and biotite gneiss with less abundant amphibolite, calc-silcate gneiss, dolomitic marble and serpentine.|11-MAY-16
39609|Oasis Metamorphics|69952|4|Described|p2 Tb.i, p5, p61-71|||Greenvale Province, Thomson Orogen. Crops out ~130 km SE of Georgetown. Originally mapped as part of Einasleigh Metamorphics (Withnall, 1989; Withnall et al., 1997). Distinguished as a separate unit (Withnall et al. 2002) on the basis of closer similarities to Cape River Metamorphics. These SHRIMP U-Pb zircon ages (Cross et al., 2015), of high temperature metamorphism and lower-temperature hydrothermal alteration respectively, were confirmed by age determinations using titanite: 1589 +/- 10 Ma and 456 +/- 12 Ma. The Oasis Metamorphics may, therefore, correlate with similar rocks in the Einasleigh Metamorphics W of the Lynd Mylonite Zone. Further, this unit appears to contain elements of Paleoproterozoic basement interfolded with late Neoproterozoic to Cambrian rocks.|1602 +/- 9 Ma; 459 +/- 30 Ma.|||Is intruded by Lynwater Complex.|Mainly upper amphibolite grade gneiss and amphibolite; also three sub-units: calc-silicate gneiss, amphibolite with minor biotite schist; biotite gneiss with less abundant amphibolite, calc-silicate gneiss, dolomitic marble and serpentinite.|
39609|Oasis Metamorphics|70744|5|Briefly described|p937, p939, p943, p947|Paleozoic|Neoproterozoic|Lynd Mylonite Zone, Greenvale Province. Some sediment derived from Mesoproterozoic rocks. U-Pb zircon age of peak metamorphism and igneous activity by Fergusson et al. (2007).|c.476 Ma (estimated from Fig.7).|||Thrust over Einasleigh Metamorphics.||
39609|Oasis Metamorphics|70749|5|Briefly described|p43|Cambrian|Cambrian|Greenvale Province.|~520 Ma (maximum depositional age).|||||
39609|Oasis Metamorphics|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Greenvale Province, Thomson Orogen. Core analysis indicates maximum depositional age of ~520 Ma. Metamorphic rims dated at 476+\-5 Ma, indicating metamorphic age and minimum depositional age.|<520 Ma|||||
39609|Oasis Metamorphics|73425|6|Mentioned|p2, 16|Neoproterozoic|Neoproterozoic|Greenvale Province, Thomson Orogen. Early Ordovician metamorphic rims on zircon.||||||
36271|Obree Point Volcanics|23423|4|Described|p308 Table 7.3|Early Permian|Late Carboniferous|Age: 299 +/- 6 Ma (U-Pb, zircon, SHRIMP). Intruded by Bunk Creek Granite. Also see p238. Kennedy Igneous Province.||||||
36271|Obree Point Volcanics|23430|5|Briefly described|p490|||Dated 299 +/- 6 Ma. Kennedy Province.||||||
36271|Obree Point Volcanics|23511|5|Briefly described|Map Legend||Carboniferous|||||||
36271|Obree Point Volcanics|50630|5|Briefly described|Map Legend|Permian|Late Carboniferous|Age: 299 +/- 6Ma (SHRIMP).  Dacite lava, subordinate andesite lava, boulder conglomerate, andesitic to dacitic tuff, lapilli tuff, volcanic breccia.||||||20-APR-18
36271|Obree Point Volcanics|60425|3|Fully described|p50 Tb. 3, p71|Early Permian|Late Carboniferous|Age: 299+/-6Ma.Thickness: >250m? Intruded /hornfelsed by Bunk Ck Granite. Dk. grey, mod'ly to highly porphyritic dacite lava - flow-banded/locally autobrecciated; subord. andesite lava, boulder conglom., andesitic-dacitic tuff, lapilli tuff, volc.breccia||||||07-FEB-11
36271|Obree Point Volcanics|68553|6|Mentioned|Map legend|Early Permian|Late Carboniferous|||||||
36271|Obree Point Volcanics|69030|5|Briefly described|p6|Permian|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.|299 +/- 6 Ma (SHRIMP).|||||
36271|Obree Point Volcanics|69593|5|Briefly described|p480, p483|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Scattered outcrops in eastern Hodgkinson Province.|299 +/- 6 Ma (SHRIMP: Garrad and Bultitude, 1999).||||Dacite and rhyolite, minor andesite lava and tuffaceous rocks, possibly intrusive in part.|
36271|Obree Point Volcanics|70207|6|Mentioned|p74|Permian|Late Carboniferous|||||||
36271|Obree Point Volcanics|70345|6|Mentioned|p3|Early Permian|Late Carboniferous|||||||
36271|Obree Point Volcanics|70673|6|Mentioned|p7|Permian|Late Carboniferous|||||||
36271|Obree Point Volcanics|72983|6|Mentioned|p15|Early Permian|Late Carboniferous|Kennedy Igneous Association.||||||
41805|Og Syenite|60481|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Coarse grained biotite syenite.||||||
41805|Og Syenite|61035|4|Described|p17 Tb. 2|Triassic|Permian|Intrudes Marlborough Metamorphics. Age: ~253Ma. Consists of coarse-grained biotite syenite.||||||07-FEB-11
41805|Og Syenite|65388|4|Described|p431-432, p70 Fig. 28, p153|Late Permian|Late Permian|Intrudes Marlborough Metamorphics. May be intruded by the Magog Gabbro [?see Magog Gabbro same page].Coarse-grained biotite syenite.||||||
41805|Og Syenite|68679|5|Briefly described|p308-309, p424, p426|Permian|Permian|Marlborough Province. 5.5 km2, in the Magog Range around Mount Og.|242 +/- 3 Ma (Ar-Ar biotite: Harbort, 2001).|||Intrudes Marlborough Metamorphics and possibly Magog Gabbro.|Coarse-grained biotite syenite.|
80902|Ogilvie Hill Diorite|69593|5|Briefly described|p512|||Jardine Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|285 Ma.||||I-type.|
78948|Okangal Quartz Monzodiorite|65388|2|Defined|p270, 253 Fig 87|Early Permian|Late Carboniferous|Auburn Arch. Replaces Okangal Granodiorite. Intrudes the Torsdale Volcanics. Age inferred. Grey, fine to medium-grained, somewhat uneven-grained clinopyroxene-biotite-hornblende quartz monzodiorite.||||||
78948|Okangal Quartz Monzodiorite|68679|5|Briefly described|p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Torsdale Volcanics.|Grey, fine- to medium-grained, somewhat uneven-grained clinopyroxene-biotite-hornblende quartz monzodiorite; texturally and compositionally heterogeneous.|
69703|Old Cork beds|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Geological region: Diamantina.||||||
69703|Old Cork beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Fluviatile and lacustrine grey mudstone, and white limestone, minor sandy siltstone, silty sandstone, calcareous sandstone; duricrusted.|
69703|Old Cork beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
69703|Old Cork beds|69599|5|Briefly described|p584, p599|Eocene|Paleocene|Old Cork Basin. Maximum thickness 78m. The limestones contains freshwater gastropods and ostracods. Capped by silcrete and laterite of the Canaway profile. RELATED UNITS (continued): Also correlated (at least partly) with Moonie, Eyre, Glendower, Edkins, Springvale and Marion Formations.||||Unconformably overlies Winton Formation. Is overlain unconformably by Mueller Sandstone. Correlated (at least partly) with Werite beds; Mueller and Moses Sandstones; see COMMENTS for more.|Dominated by limestone and mudstone, with subordinate silty sandstone, calcareous sandstone and sandy siltstone. Surface exposures are commonly silicified; contains abundant wood fragments.|
39070|Old Kolonga Gabbro|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Brownish grey, fine to medium-grained, equigranular, hornblende quartz diorite; dark-green, coarse-grained, equigranular hornblende-pyroxene gabbro.|05-SEP-14
39070|Old Kolonga Gabbro|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Hornblende quartz diorite; hornblende-pyroxene gabbro.|
23883|Old Man Rhyolite|23032|4|Described|p44||Early Carboniferous|||||||
23883|Old Man Rhyolite|23291|4|Described|p50, p98 Tb. 3.11|Late Carboniferous|Carboniferous|Intrudes the Paddock Creek Formation. Geological Province: Georgetown Region.||||||18-JUN-15
23883|Old Man Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 43. I-Type.||||||
23883|Old Man Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23883|Old Man Rhyolite|40542|6|Mentioned|p97|||||||||
23883|Old Man Rhyolite|43259|4|Described|Appendix 1,p18.||Carboniferous|||||||
23883|Old Man Rhyolite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
23883|Old Man Rhyolite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23883|Old Man Rhyolite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||07-DEC-04
23883|Old Man Rhyolite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province. In Pink Ring Dykes of the Bagstowe Ring Structure.|||||Pink to brown, porphyritic, intrusive rhyolite to biotite microgranite.|
23883|Old Man Rhyolite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Pink to brown, porphyritic, intrusive rhyolite to biotite microgranite.|
27990|Olkolo Formation|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Edward River Metamorphic Group||||||12-JAN-05
27990|Olkolo Formation|22781|4|Described|p17|Proterozoic|Proterozoic|Edward River Metamorphic Group||||||
27990|Olkolo Formation|23420|5|Briefly described|p 142 table 4.4|||In the Edward River Metamorphic Group. Thickness 700m. Correlates with Dinah Formation.||||||
27990|Olkolo Formation|43596|4|Described|p16, p20 Tb. 1||Proterozoic|Of the Edward River Metamorphic Group.Conformable on Potallah Formation; conformable beneath Drovers Lagoon Formation. Thickness: up to 700m. Characterised by pink  to medium grey, partly recrystallised, fine- to medium-grained quartzite.||||||15-JAN-09
27990|Olkolo Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Edward River Metamorphic Group||||||24-JAN-05
27990|Olkolo Formation|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. 700m thick.||Edward River Metamorphic Group.||Partly correlates with Dinah Formation.|Metasiltstone, quartzite, slate, phyllite, garnet-mica schist; locally graphitic.|
23885|Olsens Granite|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Muscovite-biotite granite.||||||02-JUL-04
23885|Olsens Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Esmeralda Supersuite. Geological Province: Georgetown Region.||||||13-MAY-15
23885|Olsens Granite|23430|6|Mentioned|456p|||||||||
23885|Olsens Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 805. S-Type.||||||
23885|Olsens Granite|24197|5|Briefly described|p79 Tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Esmeralda Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Croydon Province).||||||07-FEB-11
23885|Olsens Granite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23885|Olsens Granite|40659|6|Mentioned|p250|||||||||
23885|Olsens Granite|40860|6|Mentioned|Fig.1|||See also Fig.2||||||
23885|Olsens Granite|40954|6|Mentioned|p133|||||||||
23885|Olsens Granite|43259|4|Described|Appendix 1,p52.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
23885|Olsens Granite|50537|5|Briefly described|p1.1, 1.5, 3.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Esmeralda Supersuite.||||||
23885|Olsens Granite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Very coarse to fine-grained, muscovite-biotite granite; porphyritic in part.||||||
23885|Olsens Granite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to fine-grained muscovite-biotite granite, porphyritic in part; fine- to very fine-grained granite, microgranite; commonly melanocratic.|
23885|Olsens Granite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to fine-grained muscovite-biotite granite, porphyritic in part; fine- to very fine-grained granite, microgranite; commonly melanocratic.|
23885|Olsens Granite|68355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to fine-grained muscovite-biotite granite, porphyritic in part; fine- to very fine-grained granite, microgranite; commonly melanocratic.|
23885|Olsens Granite|68356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Esmeralda Supersuite.|||Very coarse- to fine-grained muscovite-biotite granite, porphyritic in part; fine- to very fine-grained granite, microgranite; commonly melanocratic; greisen.|
23885|Olsens Granite|69591|5|Briefly described|p75, p83|||Westernmost Georgetown Inlier.||Esmeralda Supersuite.||Intrudes Croydon Volcanic Group.||
35142|Olympus Granite|23042|5|Briefly described|p76, Fig 2|Permian|Carboniferous|||||||
35142|Olympus Granite|60475|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Pink to grey, medium grained, sparsley porphyritic, biotite quartz monzonite.||||||
35142|Olympus Granite|61035|4|Described|p10 Tb. 1|Early Carboniferous|Early Carboniferous|Intrudes Mountain View Volcanics and faulted against Carmila beds. Geological Province: Connors Sudprovince. Pink to grey, medium-grained, sparsely porphyritic, biotite quartz monzonite.||||||07-FEB-11
35142|Olympus Granite|65388|2|Defined|p357-358, p90 Fig. 37, p94, 399|Late Carboniferous|Late Carboniferous|Connors Arch pluton.  Intrudes Mountain View Volcanics. Faulted against Carmila beds. Tentative age given. Pink to grey, medium-grained, sparsely porphyritic biotite quartz monzonite to granite in type section. ||||||
35142|Olympus Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Toobier, Tooloombah Creek and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
35142|Olympus Granite|68679|6|Mentioned|p347|Carboniferous|Carboniferous|Northern New England Orogen.||||||
22590|One Mile Creek Granite|22845|6|Mentioned|p49,54||Triassic|||||||
22590|One Mile Creek Granite|44923|5|Briefly described|Map Legend||Triassic|||||||
22590|One Mile Creek Granite|68679|5|Briefly described|p332, p409, p411|Late Triassic|Late Triassic|Northern New England Orogen. Outcrop area <1 km2.||||Intrudes Mount Clara beds.|Hornblende-biotite granodiorite.|
27528|Ooramera Volcanics|23799|6|Mentioned|p109|||Garnetiferous unit.||||||
27528|Ooramera Volcanics|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
27528|Ooramera Volcanics|30654|4|Described|p49|||See also P55. Lower Triassic||||||
27528|Ooramera Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
27528|Ooramera Volcanics|34543|6|Mentioned|p98|||||||||
27528|Ooramera Volcanics|37618|6|Mentioned|Fig.1|||||||||
27528|Ooramera Volcanics|38391|6|Mentioned|p9|||||||||
27528|Ooramera Volcanics|38402|6|Mentioned|p72|||||||||
27528|Ooramera Volcanics|39445|5|Briefly described|Table 9|||||||||
27528|Ooramera Volcanics|39505|6|Mentioned|p167|||||||||
27528|Ooramera Volcanics|41736|6|Mentioned|p115|||||||||
27528|Ooramera Volcanics|41738|1|Redefined|p173|Late Triassic||||||||
27528|Ooramera Volcanics|41778|6|Mentioned|Fig.2|||||||||
27528|Ooramera Volcanics|42054|6|Mentioned|p273|||||||||
27528|Ooramera Volcanics|42894|6|Mentioned|p23|||||||||
27528|Ooramera Volcanics|44750|5|Briefly described|p12,15||Early Triassic|||||||
27528|Ooramera Volcanics|44752|14|Not recorded|Fig. 43,p300||Triassic|Unconformably overlies Kin Kin Phyllite.||||||
27528|Ooramera Volcanics|44753|14|Not recorded|p47,51,52||Triassic|||||||
27528|Ooramera Volcanics|44785|14|Not recorded|p149||Early Triassic|||||||
27528|Ooramera Volcanics|44786|14|Not recorded|p193-202||Early Triassic|||||||
27528|Ooramera Volcanics|45440|2|Defined|p.14,24,25,26|||Tb.1. Of many pages. Lower Triassic?||||||
27528|Ooramera Volcanics|63821|5|Briefly described|p22|||Originally defined by Ellis (1968). Redefined by Cranfield (1994) after discovering a fault between the andesitic volcanics; now considered to be part of Brooweena Formation. Garnet-bearing tuff, rhyolitic pyroclastics and flows, sandstone and siltstone.||||||07-FEB-11
27528|Ooramera Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
27528|Ooramera Volcanics|68679|5|Briefly described|p312-313, p434, p439|Late Triassic|Late Triassic|Maryborough area, northern New England Orogen. Occurs ~25km E of the Mungore Caldera. Formerly (Ellis, 1968) included andesites; now restricted to felsic volcanics in the Stoney Range. Boundaries are faulted. 20-50m thick. ||||Correlated with Dadamarine Rhyolite (but not included in the Aranbanga Volcanic Group).|Rhyolitic agglomerate, spherulitic rhyolite, tuff and sediments; tuff is pyroclastic with plagioclase, tuffaceous clasts and pumice in a (formerly) glassy groundmass, locally contains red garnet, and is overlain by a sandstone/siltstone succession.|
27528|Ooramera Volcanics|73450|6|Mentioned|p34|||||||Equivalent to Aranbanga Volcanic Group.||
76905|Oorindimindi Gneiss|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event.||Of Williams Supersuite.|||Medium to coarse-grained gneissic granodiorite.|
76905|Oorindimindi Gneiss|69591|5|Briefly described|p59|||Maramungee area.|||||Medium- to coarse-grained gneissic granodiorite.|
76905|Oorindimindi Gneiss|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Medium to coarse-grained gneissic granodiorite.|05-MAY-16
76905|Oorindimindi Gneiss|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Medium to coarse grained gneissic granodiorite.
|
81935|Ooroonoo Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1583+/-4.3 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
23886|Ootann Granite|23291|4|Described|p102 Tb. 3.13|Early Permian|Late Carboniferous|Of the Ootann Suite. Intrudes Kitchener Granite(?), Martin Creek Microgranite; intruded by Stirlington Granite(?). Age: 296-304Ma; 299+/-2Ma; 301+/-2Ma. Geological Province: Georgetown Region.||||||25-JUN-15
23886|Ootann Granite|23423|5|Briefly described|p243||Carboniferous|Age: ~300 Ma.  Ootann Supersuite.||||||
23886|Ootann Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Age: 301 +/-2Ma K-Ar.  Ootann Supersuite||||||
23886|Ootann Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~304 Ma, Rb-Sr. Of Ootann Supersuite.||||||01-JUN-09
23886|Ootann Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 313. I-Type.||||||
23886|Ootann Granite|23616|6|Mentioned|p74|||Of Ootann Supersuite. Hodgkinson Province and Dargalong Province.||||||
23886|Ootann Granite|39564|6|Mentioned|Table 5|||||||||
23886|Ootann Granite|39997|6|Mentioned|p165|||||||||
23886|Ootann Granite|43060|5|Briefly described|p100|||||||||
23886|Ootann Granite|43083|5|Briefly described|p255|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
23886|Ootann Granite|43087|2|Defined|p38|Early Permian|Late Carboniferous|Of Ootann Suite of Richards (1981) and Ootann Supersuite of Champion (1991).||||||
23886|Ootann Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite). Medium grey to pink, medium to coarse, even-grained biotite granite.||||||01-JUN-09
23886|Ootann Granite|43259|4|Described|Appendix 1,p38.||Late Carboniferous|Rb-Sr age is 301-302 Ma. K-Ar biotite ages are 299+/-2,301+/-2 Ma.||||||01-JUN-09
23886|Ootann Granite|43626|6|Mentioned|p10|||||||||
23886|Ootann Granite|60425|4|Described|p73, p278-9 Appdx. |Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite). Age:~304Ma (Rb-Sr), 301+/-2Ma, 299+/-2Ma (K-Ar). I-type. Med.-coarse-gr., even-gr.hornblende biotite granite and minor granodiorite; rounded mafic enclaves (to ~30cm) common; slightly-moderately altered in places||||||07-FEB-11
23886|Ootann Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A third age is 301-302 Ma (Rb-Sr, biotite).|299 +/- 2 Ma, 301 +/- 2 Ma (K-Ar, biotite).|Unit in Ootann Supersuite.|||Pale pink to pale greyish pink, medium-grained, uneven-grained to porphyritic hornblende-biotite and biotite monzogranite; mafic inclusions (to ~30 cm) common.|
23886|Ootann Granite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|305 Ma.|Ootann Supersuite.||||
29320|Ootann Suite|23291|4|Described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||26-MAR-15
29320|Ootann Suite|23624|6|Mentioned|p9|||Superseded by the Ootann Supersuite.||||||08-JUL-15
29320|Ootann Suite|43087|6|Mentioned|p31|||Variation on Ootann Supersuite?||||||
29320|Ootann Suite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Ootann Supersuite.||||||26-MAR-15
29320|Ootann Suite|60425|5|Briefly described|p276-7 Appdx.|Early Permian|Late Carboniferous|Of the Ootann Supersuite. Includes ~30 named granites. I-types.||||||07-FEB-11
29320|Ootann Suite|62523|5|Briefly described|Map legend at p3-5|Early Permian|Late Carboniferous|Of the Ootann Supersuite. Contains Little Watson Granite.||||||07-FEB-11
29320|Ootann Suite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Ootann Supersuite.|Ootann Granite.|||
36232|Opah Granite|23423|5|Briefly described|p314 table 7.4|||||||||
36232|Opah Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|O'Briens Creek Supersuite.||||||
36232|Opah Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36232|Opah Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36232|Opah Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 358. I-Type.||||||
36232|Opah Granite|23616|6|Mentioned|Table 3 p55|||See also p100 Appendix 2. Of O'Briens Creek Supersuite.||||||
36232|Opah Granite|23624|4|Described|p20|||Parent: O'Brien's [misspelling of O'Briens] Creek Supersuite.||||||08-JUL-15
36232|Opah Granite|60425|4|Described|p51 Tb. 3, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Lappa Suite (O'Briens Creek Supersuite). Cuts into Claret Creek Volcanics. Pink-cream, fine- to med.-grained, even-grained to porphyritic leucocratic biotite granite; some porphyritic biotite microgranite. I-type.||||||07-FEB-11
36232|Opah Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink to cream, fine- to medium-grained, even-grained to porphyritic, leucocratic biotite granite.|
36232|Opah Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink to cream, fine- to medium-grained, even-grained to porphyritic, leucocratic biotite granite.|
36232|Opah Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink to cream, fine- to medium-grained, even-grained to porphyritic, leucocratic biotite granite.|
22602|Orient Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
22602|Orient Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
22602|Orient Rhyolite|23513|5|Briefly described|Map legend||Late Carboniferous|Palaeozoic Volcanic No. V92. I-Type.||||||
22602|Orient Rhyolite|23616|5|Briefly described|Table 3 p49||Carboniferous|Of Boonmoo Volcanic Subgroup||||||
22602|Orient Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
22602|Orient Rhyolite|43259|4|Described|Appendix 1,p9.||Late Carboniferous|Of Boonmoo Volcanic Subgroup.||||||
22602|Orient Rhyolite|43567|5|Briefly described|Table 2,p401|||||||||
22602|Orient Rhyolite|43626|2|Defined|p19|||Rb-Sr Age: 313 Ma.||||||06-SEP-18
22602|Orient Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22602|Orient Rhyolite|60425|5|Briefly described|p48 Tb. 3|Late Carboniferous|Late Carboniferous|Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
27529|Orion Formation|24077|6|Mentioned|p412 Fig. 8|||Geological Province: Bowen Basin.||||||
27529|Orion Formation|29721|6|Mentioned|Table 65|||||||||
27529|Orion Formation|30545|6|Mentioned|Fig.2|||Lower Permian age||||||
27529|Orion Formation|30546|6|Mentioned|p107|||Correlation.Lower Permian age||||||
27529|Orion Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27529|Orion Formation|30915|6|Mentioned|p98|||||||||
27529|Orion Formation|33366|6|Mentioned|Fig.3|||Perm.||||||
27529|Orion Formation|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
27529|Orion Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
27529|Orion Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
27529|Orion Formation|36739|6|Mentioned|Fig.5|||||||||
27529|Orion Formation|39445|5|Briefly described|Table 7|||See also Table 8||||||
27529|Orion Formation|39994|6|Mentioned|p200|||||||||
27529|Orion Formation|42250|6|Mentioned|Fig.3 P30|||||||||
27529|Orion Formation|43987|14|Not recorded|p270|||Freshwater sediments.||||||
27529|Orion Formation|43990|14|Not recorded|Map Legend|||Part of Reids Dome Beds.||||||
27529|Orion Formation|43994|14|Not recorded|Map Legend|||||||||
27529|Orion Formation|44170|14|Not recorded|p8|||||||||
27529|Orion Formation|44172|14|Not recorded|p1323,Fig.2,T.1,1331||Sakmarian|Represents Reids Dome Beds in Springsure area.||||||
27529|Orion Formation|44173|14|Not recorded|p110-112||Early Permian|||||||
27529|Orion Formation|44218|14|Not recorded|p19||Sakmarian|||||||
27529|Orion Formation|44337|5|Briefly described|Map Legend||Early Permian|Lithology.||||||
27529|Orion Formation|44422|14|Not recorded|p151,152||Early Permian|||||||
27529|Orion Formation|45071|3|Fully described|Table 1|||||||||
27529|Orion Formation|48900|4|Described|p25|||Lower Permian||||||
27529|Orion Formation|70030|5|Briefly described|p192|Mesoarchean|Mesoarchean|Geological province: Murchison Domain, Yilgarn Craton.||Unit of Mount Gibson Group.||Overlain by Golden Grove Formation.||
35392|Ormoral Volcanics|61392|4|Described|p163-165, p167|Middle Devonian|Early Devonian|Of Silverwood Group (Keinjan Terrane). Consists of high-level mafic intrusive rocks, subaqueous mafic extrusives, syn-eruptive hydroclastic facies, resedimented subaerial lapillistones and proximal high-density turbidites. Max. thickness: 620m||||||07-FEB-11
35392|Ormoral Volcanics|63731|5|Briefly described|Map legend|Devonian|Silurian|Of Silverwood Group. Almalgamated volcaniclastic arenite, basaltic to andesitic lavas and volcaniclastic arenite and siltstone with interbedded peperite.||||||
35392|Ormoral Volcanics|63748|4|Described|p7 Fig. 3, p8|Middle Devonian|Middle Devonian|Of Silverwood Group. Conformable on Bald Hill Fm. Max.thickness: ~620m. Geol.Prov:Silverwood province. Include dolerite, anorthosite, basalt, basaltic andesite + backarc andesite.||||||07-FEB-11
35392|Ormoral Volcanics|68679|5|Briefly described|p445-447|Middle Devonian|Middle Devonian|Van Noord (1999). Silverwood Province. Low-K tholeiitic submarine extrusives. Up to ~620m thick. Deposited in a deep-marine intra-arc basin. Unfossiliferous.||Silverwood Group.||Conformably overlies Bald Hill Formation. Is overlain unconformably by Bromley Hills Formation.|Hypabyssal rocks include dolerite, anorthosite, basalt, basaltic andesite and andesite. Extrusive rocks include pillow lava, hyaloclastite and peperite sporadically interbedded with proximal, epiclastic high-density turbidites.|
35392|Ormoral Volcanics|73600|6|Mentioned|p204|Devonian|Devonian|New England Orogen.||||||
24445|Oroopo Metabasalt|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
24445|Oroopo Metabasalt|24419|5|Briefly described|p16, p12 Fig. 4, p13 Fig. 5|Proterozoic|Proterozoic|Of the Haslingden Group.  Basalt lava flows with mainly arenaceous sedimentary intercalations. Unconformably overlies Saint Ronans Metamorphics, Kallala Quartzite and Sulieman Gneiss. See also p15 Fig. 6.||||||09-MAR-05
24445|Oroopo Metabasalt|37862|4|Described|p587|||||||||
24445|Oroopo Metabasalt|38234|4|Described|p103|||||||||
24445|Oroopo Metabasalt|38442|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24445|Oroopo Metabasalt|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24445|Oroopo Metabasalt|38658|6|Mentioned|p153|||||||||
24445|Oroopo Metabasalt|39445|5|Briefly described|Table 2|||||||||
24445|Oroopo Metabasalt|39622|6|Mentioned|p19|||||||||
24445|Oroopo Metabasalt|40840|6|Mentioned|Map legend|||||||||
24445|Oroopo Metabasalt|41978|6|Mentioned|p501|||||||||
24445|Oroopo Metabasalt|42565|4|Described|Table 1 P6|||||||||
24445|Oroopo Metabasalt|45161|4|Described|p11|||See also Table 2||||||
24445|Oroopo Metabasalt|45166|4|Described|p16|||||||||
24445|Oroopo Metabasalt|49009|2|Defined|p33|Precambrian|Precambrian|Mapped as Eastern Creek Volc. & Sybella Gr. by Noakes & others (1959).||||||
24445|Oroopo Metabasalt|49041|5|Briefly described|Table 1|||||||||
24445|Oroopo Metabasalt|50536|6|Mentioned|p4.1|||Geological Province: Mount Isa Inlier.||||||
24445|Oroopo Metabasalt|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metabasalt, meta-arenite, metasiltstone, limestone.||||||
24445|Oroopo Metabasalt|64250|6|Mentioned|p11 fig 3|||Western Fold Belt, Mount Isa Inlier.||||||
24445|Oroopo Metabasalt|65387|6|Mentioned|p3 Tb.1a|||[Mis-spelt as Oroopoo Metabasalt.] Western succession. Samples submitted but did not yield sufficient zircons for SHRIMP analysis.|||||Includes felsic volcanics.|
24445|Oroopo Metabasalt|65396|6|Mentioned|p82, p175, p241|Statherian|Statherian|Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform.||||||
24445|Oroopo Metabasalt|67323|5|Briefly described|GIS attrib tbl,  p7-8, p39, p107|Paleoproterozoic|Orosirian|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Post-Barramundi basement. Ardmore - May Downs Domain, Mount Isa Inlier. Maximum depositional age of 'felsic' material 1857 +/-7 Ma.||||Intruded by the Yarrie Rock Waterhole Granite. Unconformably overlain by Mount Isa Group.|Metabasalt, metamorphosed calcareous sandstone.|
24445|Oroopo Metabasalt|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, as well as Bucket Hole Metavolcanics, Alpha Centauri Metamorphics and Kallala Quartzite, are all mapped under the symbol, -Pvo.||||||25-JUL-13
24445|Oroopo Metabasalt|68575|5|Briefly described|p1, p6-7, p94-100, p125, p134|||Mount Isa Region. Age from contaminating crustal contamination (sourced from underlying North Australian Craton crust) during ascent: discussion as to the volcanic or sedimentary nature of the zircons. Previous equating of this unit with the Eastern Creek Volcanics is thrown into doubt. Whole rock Sm-Nd isotopic data and age (1857 Ma)."|1857 +/- 7 Ma (maximum extrusion age).||||Basalt, intermediate and possible felsic volcanics.|
24445|Oroopo Metabasalt|69591|5|Briefly described|p29-30, p32, p42, p58|Paleoproterozoic|Paleoproterozoic|Ardmore-May Downs Domain, Mount Isa Province. Has been equated with Eastern Creek Volcanics (Bultitude, 1982).|~1857 Ma (maximum detrital age).|||Is overlain unconformably by Mount Isa Group. (Possibly) correlated with Edmirringee Volcanics.|Metabasalt, metamorphosed calcareous sandstone. Includes a fine-grained siliceous metasedimentary interval (see AGE).|
24445|Oroopo Metabasalt|71592|5|Briefly described|Appendix A.||Orosirian|Mount Isa Orogen.|1857+/-7 Ma (MDA: U-Pb zircon SHRIMP)|||||
24445|Oroopo Metabasalt|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
24445|Oroopo Metabasalt|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Mafic extrusives.|
28023|Oswald Schist|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
28023|Oswald Schist|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
28023|Oswald Schist|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
28023|Oswald Schist|43596|3|Fully described|p9-10, p21 Tb. 1||Proterozoic|Age of two-mica granite: ~: 1585 Ma (SHRIMP).In Yambo Inlier. Intruded by Aralba, Wongu and Burton Lagoon Granites and several others also. detailed lithological information included for this two-mica schist.||||||18-FEB-19
28023|Oswald Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|Yambo Metamorphic Group||||||24-JAN-05
28023|Oswald Schist|50537|5|Briefly described|p6.1|Mesoproterozoic|Mesoproterozoic|Age: 1585Ma (SHRIMP). Geological Province: Yambo Inlier.||||||20-MAR-13
28023|Oswald Schist|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3, p102|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Is intruded by the Cape York Peninsula Batholith.||Yambo Metamorphic Group.||Is faulted against Annie Creek and Saraga Schists.||
28023|Oswald Schist|73083|6|Mentioned|p67|Mesoproterozoic|Mesoproterozoic|||||||
26091|Overhang Jaspilite|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Mary Kathleen Group. Calcareous siltstone, sandstone, quartzite, limestone, jaspilite. Underlies Answer Slate. Overlies Mitakoodi Quartzite.||||||18-JAN-07
26091|Overhang Jaspilite|22460|5|Briefly described|p447|||Of the Mary Kathleen Group.||||||18-JAN-07
26091|Overhang Jaspilite|22461|5|Briefly described|Fig 1 p464|||Also see Fig 2 p466 and p465.||||||
26091|Overhang Jaspilite|23064|6|Mentioned|135|||Geol province Mt Isa Inlier. Of the Mary Kathleen Group.||||||06-FEB-07
26091|Overhang Jaspilite|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|||||||
26091|Overhang Jaspilite|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Ballara Quartzite. Overlain by Corella Formation. Geological Province: Eastern Fold Belt.||||||
26091|Overhang Jaspilite|29965|6|Mentioned|p403|||||||||
26091|Overhang Jaspilite|29969|6|Mentioned|Table 1|||||||||
26091|Overhang Jaspilite|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26091|Overhang Jaspilite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mary Kathleen Group.  Interfingers with Corella Formation.||||||25-AUG-04
26091|Overhang Jaspilite|30530|6|Mentioned|p516|||||||||
26091|Overhang Jaspilite|30531|2|Defined|p17|Precambrian|Precambrian|||||||
26091|Overhang Jaspilite|32660|5|Briefly described|Table 5|||||||||
26091|Overhang Jaspilite|32959|6|Mentioned|Fig.21|||||||||
26091|Overhang Jaspilite|33900|5|Briefly described|p17|||||||||
26091|Overhang Jaspilite|35074|6|Mentioned|Fig.2|||||||||
26091|Overhang Jaspilite|35295|6|Mentioned|p603|||||||||
26091|Overhang Jaspilite|37568|5|Briefly described|p81|||||||||
26091|Overhang Jaspilite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26091|Overhang Jaspilite|37862|6|Mentioned|p587|||||||||
26091|Overhang Jaspilite|38234|6|Mentioned|Fig.2|||||||||
26091|Overhang Jaspilite|38235|6|Mentioned|p113|||||||||
26091|Overhang Jaspilite|38276|6|Mentioned|Fig.1|||||||||
26091|Overhang Jaspilite|38350|4|Described|p11|||||||||
26091|Overhang Jaspilite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26091|Overhang Jaspilite|38833|6|Mentioned|p161|||||||||
26091|Overhang Jaspilite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26091|Overhang Jaspilite|39445|6|Mentioned|p36|||See also p42 and Table 2.||||||06-FEB-07
26091|Overhang Jaspilite|39496|4|Described|p8|||||||||
26091|Overhang Jaspilite|39622|6|Mentioned|Fig.2|||||||||
26091|Overhang Jaspilite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
26091|Overhang Jaspilite|40840|6|Mentioned|Map legend|||||||||
26091|Overhang Jaspilite|41306|6|Mentioned|p12|||||||||
26091|Overhang Jaspilite|41761|6|Mentioned|p286|||||||||
26091|Overhang Jaspilite|41791|4|Described|p248|||||||||
26091|Overhang Jaspilite|41978|6|Mentioned|p491|||||||||
26091|Overhang Jaspilite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Siltstone, chert, limestone, jaspilite.||||||09-FEB-09
26091|Overhang Jaspilite|45136|3|Fully described|p28|||||||||
26091|Overhang Jaspilite|45161|4|Described|p42|||||||||
26091|Overhang Jaspilite|45166|5|Briefly described|p23|||||||||
26091|Overhang Jaspilite|46801|6|Mentioned|Fig. 14|||Stratigraphy.||||||
26091|Overhang Jaspilite|46962|4|Described|Table 1|||See also Fig.3.||||||
26091|Overhang Jaspilite|49009|6|Mentioned|p4|||See also p45.||||||06-FEB-07
26091|Overhang Jaspilite|49041|6|Mentioned|p6|||||||||
26091|Overhang Jaspilite|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Consists of thinly bedded calcareous and cherty rocks, some stromatolitic; manganiferous unit included.  Conformably on the Mitakoodi Quartzite.  Marker unit. Geological Province: Eastern Fold Belt Province.  See also p81.||||||18-JAN-07
26091|Overhang Jaspilite|50125|6|Mentioned|p89|||Geological Province: Eastern Succession, Mount Isa Inlier||||||
26091|Overhang Jaspilite|50332|5|Briefly described|p16, p18, p88, p96|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Conformably underlain by Mitakoodi Quartzite. Consists of thinly bedded calcareous and cherty rocks, some of which are stromatolitic.||||||07-FEB-11
26091|Overhang Jaspilite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Calcareous siltstone, arenite, chert, limestone, jaspilite, ironstone.||||||
26091|Overhang Jaspilite|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Eastern Fold Belt.||||||03-JUN-09
26091|Overhang Jaspilite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1750Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
26091|Overhang Jaspilite|61922|6|Mentioned|p8, p16 Fig. 8|||The Mitakoodi Quartzite has been thrust over this unit (Bulonga Thrust).  Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
26091|Overhang Jaspilite|61925|4|Described|p56 Fig. 1, p 57 Fig. 3, p60, p62|Paleoproterozoic|Paleoproterozoic|Interbedded seq.of variably ferruginous and calcareous siltstone and limestone-marl incl.bands of red jasper. Age near base of overlying unit:1742+/-6Ma. Both conformable and unconformable on upper Mitakoodi Quartzite. Max.thick:1200m. Geol.Prov: Leichardt Superbasin||||||19-MAR-18
26091|Overhang Jaspilite|61926|5|Briefly described|p70-71, p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Interbedded jasper, chert, magnetite, calc-silicate, dolomite, minor muscovite-biotite schist. Age: 1742+/-6Ma. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||07-NOV-08
26091|Overhang Jaspilite|61936|5|Briefly described|p190 Fig. 3|||Overlies Mitakoodi Quartzite. Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
26091|Overhang Jaspilite|63593|6|Mentioned|p288 Fig.2. |||500 m thick.|Between c.1840 and 1800 Ma.||||Siltstone, limestone, jasperite.|
26091|Overhang Jaspilite|64068|6|Mentioned|p46.|Paleoproterozoic|Paleoproterozoic|||||Is unconformably overlain by Little Burke Tillite.||05-APR-12
26091|Overhang Jaspilite|64248|6|Mentioned|p38 Fig.5||||<1756 +/- 3 Ma.|||Overlies Mitakoodi Quartzite. Is overlain by Corella Formation.||11-DEC-17
26091|Overhang Jaspilite|64250|5|Briefly described|p13 fig.5, p14, p11 fig 3, p16 fig.6|||Cloncurry Fold Belt, Mount Isa Inlier. Absent in East of Mt Isa Inlier. Mis-spelt as Jasperlite in Fig.6.||Mary Kathleen Group||Overlies Mitakoodi Quartzite. Possible correlation with Corella Formation.||
26091|Overhang Jaspilite|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
26091|Overhang Jaspilite|65396|5|Briefly described|p16-17, p82, p175, p178, p180, p183,p190|Statherian|Statherian|See also p241. Eastern Fold Belt, Leichhardt Superbasin. Cover Sequence 3. Appears as Overhang Jasperlite on p16 and p190.||Mary Kathleen Group||Overlies Mitakoodi Quartzite; overlain by Corella Formation. Is correlated with Corella Formation.|Calcareous metasediments.|
26091|Overhang Jaspilite|66913|5|Briefly described|p170 fig 1, p172||||1700-1725 Ma|||Correlated with Staveley Formation.|Carbonate-bearing.|
26091|Overhang Jaspilite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p16, p39, p107. Mitakoodi Domain, Leichhardt Superbasin. Not dated. High magnetic susceptibility.|||Includes Chumvale Breccia.|Overlies Mitakoodi Quartzite. Folded or thrust against Corella Formation. May be partly equivalent to Corella Formation.|Predominantly grey siltstone with common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places; local jaspilitic layers.|
26091|Overhang Jaspilite|68542|6|Mentioned|p16 fig 4|||||||||
26091|Overhang Jaspilite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
26091|Overhang Jaspilite|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
26091|Overhang Jaspilite|69056|5|Briefly described|p2, p13, p53|Statherian|Statherian|See also Time-Space plot sheet, Reference images sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area. Combined with other units to form the Mitakoodi Formation, a regionally discrete unit for modelling purposes.||||Overlies Mitakoodi Quartzite. Is overlain by Corella Formation. Possibly partially equivalent to Corella Formation.|A distinctive unit of argillaceous sediments and limestone (locally stromatolitic), with prominent iron-rich jaspilite beds.|
26091|Overhang Jaspilite|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Overlies Mitakoodi Quartzite. Is intruded by Wonga Granite. Is overlain by Corella and Doherty Formations.||25-JAN-19
26091|Overhang Jaspilite|69591|4|Described|p29, p33, p35, p36 Figs.2.18 -19, p57|Paleoproterozoic|Paleoproterozoic|Uppermost unit in the Mitakoodi Domain, Leichhardt Superbasin, Mount Isa Province. Part of Quilalar Supersequence. Below wave-base shallow shelf deposits. Not dated, but may be partly equivalent to Corella Formation.|||Chumvale Breccia.|Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places; local jaspilitic layers.|
26091|Overhang Jaspilite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|An un-named sub-unit is mapped separately, comprising structurally interlayered, isoclinally folded and transposed, sparry limestone, calc-silicate, carbonate breccia, carbonatised metadolerite, quartzite, schist and meta-siltstone.||Malbon Group.|||Predominantly grey siltstone with local jaspilitic layers and common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|An un-named sub-unit is mapped separately, comprising structurally interlayered, isoclinally folded and transposed, sparry limestone, calc-silicate, carbonate breccia, carbonatised metadolerite, quartzite, schist and meta-siltstone.||Malbon Group.|||Predominantly grey siltstone with local jaspilitic layers and common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Malbon Group.||Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with local jaspilitic layers and silicified limestone.|
26091|Overhang Jaspilite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Grey siltstone with local jaspilitic layers and silicified limestone.|
26091|Overhang Jaspilite|71799|5|Briefly described|p150 fig 2, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca. 1750 Ma|||Overlies the Mitakoodi Quartzite. Overlain by the Corella Formation.|Siltstone, carbonaceous shale and dolomite.|
26091|Overhang Jaspilite|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Partially overlying siltstone, slate and phyllite of the Mitakoodi Quartzite. Shown as youngest part of the Malbon Group.||Malbon Group||Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with local jaspilitic layers and common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Partially overlying siltstone, slate and phyllite of the Mitakoodi Quartzite. Shown as youngest part of the Malbon Group.||Malbon Group||Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with local jaspilitic layers and common limestone (locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Malbon Group||Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with local jaspilitic layers and common limestone(locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Malbon Group||Overlies Mitakoodi Quartzite.|Predominantly grey siltstone with local jaspilitic layers and common limestone(locally stromatolitic and silicified with jaspilitic layers); local ironstone, banded in places.|
26091|Overhang Jaspilite|72889|6|Mentioned|p6 Fig.i.|||||||||
26091|Overhang Jaspilite|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
26091|Overhang Jaspilite|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
26091|Overhang Jaspilite|73553|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|||||||
24446|Overlander Granite|22722|6|Mentioned|p277|||||||||
24446|Overlander Granite|24197|5|Briefly described|p32, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24446|Overlander Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24446|Overlander Granite|37862|4|Described|p586|||||||||
24446|Overlander Granite|38350|4|Described|p17|||||||||
24446|Overlander Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24446|Overlander Granite|38658|6|Mentioned|p153|||||||||
24446|Overlander Granite|39445|6|Mentioned|Table 2|||||||||
24446|Overlander Granite|40840|6|Mentioned|Map legend|||||||||
24446|Overlander Granite|42879|6|Mentioned|p214|||||||||
24446|Overlander Granite|45161|5|Briefly described|p31|||||||||
24446|Overlander Granite|45166|5|Briefly described|p34|||||||||
24446|Overlander Granite|49009|2|Defined|p34|Proterozoic|Proterozoic|Mapped as Wonga Granite by Carter & Opik (1963).||||||
24446|Overlander Granite|49041|5|Briefly described|Table 2|||||||||
24446|Overlander Granite|50100|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Burstall Suite (Wonga Batholith). Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||13-OCT-08
24446|Overlander Granite|50536|5|Briefly described|p1.4, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||07-NOV-08
24446|Overlander Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Leucocratic hornblende-biotite granite.||||||
24446|Overlander Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Medium- to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite.|
24446|Overlander Granite|69591|5|Briefly described|p60|||||Burstall Suite.|||Medium- to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite.|
24446|Overlander Granite|72596|6|Mentioned|p40, 46|Statherian|Statherian|Correlated with / compositionally similar to the granitic component of the Mount Erle Complex and Myubee Igneous Complex, and the Revenue and Burstall granites (see Bultitude et al., 1982; Blake et al., 1984). Geochronologic constraint given as C. Lewis & S. Jones, GA, written communication, August, 2019.|ca. 1727 Ma|Burstall Suite||||
24446|Overlander Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Medium to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite. Coarse-grained to graphic quartz-feldspar pegmatite; minor calc-silcates.|
24446|Overlander Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Medium to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite. Coarse-grained to graphic quartz-feldspar pegmatite; minor calc-silcates.|
24446|Overlander Granite|72799|4|Described|p1, p3, p5-11|Statherian|Statherian|Mary Kathleen Domain. Geochron is new magmatic crystallisation age, which supports earlier interpretations. Forms several small elongate, sill-like plutons in the far northeast of the Duchess 1:100 000 Sheet area. Possible source of the copper mineralisation in nearby country rocks.|1740 +/- 5 Ma SHRIMP U-Pb|Burstall Suite[?]||Intrudes Corella Formation. Equivalent to Burstall Granite, Revenue Granite, and part of Myubee Igneous Complex.|Includes foliated, pale pink, fine- to medium-grained, very leucocratic granite.|
24446|Overlander Granite|73529|5|Briefly described|p1, p2 Fig.1, p4-p7, p10-11, p13-14|Statherian|Statherian|Forms part of a discontinuous 21 km long, 5 km wide, N-S trending pluton. Used to constrain timing of the proposed Wonga Orogeny based on deformation. See also Overlander granite.|1736+/-3 Ma Pb/Pb zircon|Burstall Suite||Intrudes Corella Formation|Intrusive unit.|09-MAR-23
24446|Overlander Granite|73553|4|Described|p2, p8, p37, p43-45, p64, p71|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Forms small elongate, north-trending sill-like intrusions, abundant outcrop. Included in Burstall Suite by Budd et al., (2001). Cut by numerous commonly quartz-filled faults, and scattered mafic dykes assigned to the Lakeview Dolerite (Bultiude et al., 1982a, b). High-K type granite, A-type characteristics, strongly oxidised, highly fractionated. Predominantly mottled white tones on radiometric images, very low responses on aeromagnetic images. See also p108-112, p117-118, p135, p152, p154, p164-165, p176, p221, p224, p228, p258, p266.|1740+/-5 Ma U-Pb (SHRIMP) zircon|Burstall Suite||Intrudes Corella Formation, intruded by Lakeview Dolerite|Fine- to medium-grained, even-grained to slightly porphyritic, and variably deformed, recrystallised and foliated, includes porphyritic varieties. Very leucocratic.|03-FEB-23
24447|Oweenee Rhyolite|23032|4|Described|p44||Carboniferous|||||||
24447|Oweenee Rhyolite|23422|5|Briefly described|p180, p205 Table 6.3, p217 Table 6.11|Visean|Visean|Formerly Oweenee Granite. Of Oweenee Supersuite. Intruded by the Malmesbury Microgranite.||||||14-APR-15
24447|Oweenee Rhyolite|23424|5|Briefly described|Fig 8.2 p328 Fig 8.4||Carboniferous|||||||
24447|Oweenee Rhyolite|23431|5|Briefly described|p538|||||||||
24447|Oweenee Rhyolite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
24447|Oweenee Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V56. I-Type.||||||
24447|Oweenee Rhyolite|23893|5|Briefly described|p18|Early Carboniferous|Early Carboniferous|Of Oweenee Supersuite. Originally Oweenee Granite. Geological Province: Kennedy Province.||||||14-APR-15
24447|Oweenee Rhyolite|24577|5|Briefly described|p754 Fig. 2|Late Paleozoic|Late Paleozoic|Geological Provicne: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||07-NOV-08
24447|Oweenee Rhyolite|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin.||||||06-APR-05
24447|Oweenee Rhyolite|24613|5|Briefly described|p6 Fig. 3, p113, p114|Early Carboniferous|Early Carboniferous|Of Scott (1988). Geological province: Burdekin Basin.||||||07-FEB-11
24447|Oweenee Rhyolite|41735|1|Redefined|p284|Visean||Supersedes in part published name Oweenee Granite. See also Malmesbury Microgranite.||||||
24447|Oweenee Rhyolite|41774|6|Mentioned|p32|||||||||
24447|Oweenee Rhyolite|41916|6|Mentioned|p33|||||||||
24447|Oweenee Rhyolite|42054|6|Mentioned|p273|||||||||
24447|Oweenee Rhyolite|42295|5|Briefly described|Fig.2 P5|||||||||
24447|Oweenee Rhyolite|42690|5|Briefly described|map legend|Carboniferous||||||||
24447|Oweenee Rhyolite|42692|5|Briefly described|map legend|Carboniferous||||||||
24447|Oweenee Rhyolite|42752|5|Briefly described|Fig.2 P46|||||||||
24447|Oweenee Rhyolite|42933|3|Fully described|p217|||supersedes Oweenee Granite||||||
24447|Oweenee Rhyolite|43095|3|Fully described|p37||Carboniferous|probable Middle Carboniferous age.||||||
24447|Oweenee Rhyolite|43259|4|Described|Appendix 1,p5.||Early Carboniferous|||||||
24447|Oweenee Rhyolite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
24447|Oweenee Rhyolite|60705|5|Briefly described|p649|||Welded rhyolite ignimbrites. Geological Province: Clarke River Basin.||||||12-APR-05
24447|Oweenee Rhyolite|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province, Clarke River Basin. High K, Th and U radiometric responses.|||||Rhyolitic ignimbrite; generally crystal-rich and strongly welded and recrystallised.|
24447|Oweenee Rhyolite|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province, Clarke River Basin. High K, Th and U radiometric responses.|||||Rhyolitic ignimbrite; generally crystal-rich and strongly welded and recrystallised.|
24447|Oweenee Rhyolite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Rhyolitic ignimbrite, generally crystal-rich and strongly welded and recrystallised.|
24447|Oweenee Rhyolite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Rhyolitic ignimbrite, generally crystal-rich and strongly welded and recrystallised.|
24447|Oweenee Rhyolite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
24447|Oweenee Rhyolite|68576|5|Briefly described|Q_11: p38|||Camel Creek Subprovince. Coeval with Malmesbury Microgranite. Kennedy Igneous Association. Forms hilly topography.|||||Crystal-rich rhyolitic ignimbrite.|
24447|Oweenee Rhyolite|69592|6|Mentioned|p274 Fig.4.65|Mississippian|Mississippian|||||||
24447|Oweenee Rhyolite|69593|5|Briefly described|p491, p494-496|Visean|Visean|Kangaroo Hills and Paluma Subprovinces, Kennedy Igneous Association. Forms scattered outcrops in the Townsville region. Originally mapped as a granite (Gunther and Withnall, 1992).||Oweenee Supersuite.|||I-type. Thick sheets of crystal-rich to lithic-rich rhyolitic to dacitic ignimbrite; minor tuff, lava, breccia.|
36411|Oweenee Supersuite|23422|4|Described|p166, p217 Table 6.11|Carboniferous|Carboniferous|||||||
36411|Oweenee Supersuite|23424|5|Briefly described|p339|||Ingham Batholith.||||||
36411|Oweenee Supersuite|23430|5|Briefly described|p489||Carboniferous|Age: SHRIMP 337+/-7 Ma.||||||21-APR-09
36411|Oweenee Supersuite|23617|5|Briefly described|Table 3 p52||Carboniferous|Age: Rb-Sr 342 +/- 7 Ma. Also see Figure 4 p8-9. Ingham Batholith. Kennedy Province.||||||21-APR-09
36411|Oweenee Supersuite|23893|5|Briefly described|p17|Visean|Visean|Geological Province: Kennedy Province.||||||
36411|Oweenee Supersuite|63154|5|Briefly described|p285 Fig. 5|Early Carboniferous|Early Carboniferous|Geological province: Charters Towers Province.||||||
36411|Oweenee Supersuite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit (in part), as well as the Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Almaden Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||
36411|Oweenee Supersuite|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Graveyard Creek Subprovince (Broken River Province).|||||I-type granitoids.|
36411|Oweenee Supersuite|69593|3|Fully described|p484, p491-494, p496-497, p504|||Gunther and Withnall (1992, 1995). Ingham region. Crops out mainly W of the (interpreted extension of) Palmersville Fault. Has similarities with Ootann Supersuite. Includes several highly fractionated units. Miarolitic cavities imply high-level emplacement; intrusive and extrusive phases are comagmatic.  Associated with significant tin mineralisation (eg Kangaroo Hills Mineral Field). CONSTITUENTS (continued): May also include Paluma and Watershed North Rhyolites.|~345-330 Ma.||Oweenee Rhyolite; Malmesbury, Clemant Microgranites; Baumans Camp, Macauley Creek, Spinifex, Coane Range, Kallanda, Rollingstone, Rockingham Bay, White Crystal, Poison Creek Granites. See COMMENTS.||I-type. Seriate to porphyritic biotite and lesser hornblende-biotite granite and microgranite; subordinate hornblende-biotite diorite to granodiorite in places.|
36411|Oweenee Supersuite|73425|6|Mentioned|p3|||||||||
29615|Owens Knob Suite|43005|5|Briefly described|p216|||||||||
36315|P"" Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36315|P"" Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Shown as 'P' Granite.||Unit in Ootann Supersuite.|||Pink, fine- to coarse-grained biotite monzogranite; minor microgranite.|20-AUG-15
38884|Pack Granite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
38884|Pack Granite|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
38884|Pack Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgpa].  Pink, medium-grained leucocratic muscovite-biotite granite.||||||
38884|Pack Granite|50197|5|Briefly described|Map Legend|Triassic|Permian|||||||
38884|Pack Granite|68008|3|Fully described|p332, p334, p339, p418-419|Triassic|Permian|Originally mapped by Troensegaard (1969) who named two outcrops as the Crow Creek granite. 35km SW 0f Calliope. Total outcrop area c. 1 km2, forming the southern flanks of Mount Pack from which the name is taken. The type area is along Crow Creek, a tributary of Dan Dan Creek. Forms fairly steep hills. Geophysice briefly described. Geochemistry described. No age determination. Source of gold in a sulphide-bearing quartz vein as well as alluvial workings in Crow Creek.||||Intrudes Rockhampton Group and Mount Alma Formation.|Pink, medium-grained, equigranular, leucocratic muscovite-biotite granite to granodiorite, with closely spaced joints.|
38884|Pack Granite|68679|5|Briefly described|p425, p427|||Yarrol Province. Occurs as two small areas, ~1 km2, just NE of the Mount Seaview Igneous Complex. Geochemistry briefly described.||||Intrudes Rockhampton Group and Mount Alma Formation.|Leucocratic muscovite-biotite granite.|
36557|Packhorse Creek granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 222.  I-Type.||||||
23889|Paddock Creek Formation|23032|4|Described|p42||Carboniferous|||||||
23889|Paddock Creek Formation|23291|5|Briefly described|42, p91 Tb. 3.8p|Carboniferous|Carboniferous|Intruded by Bagstowe Granite and Old Man Rhyolite. Parent: Butlers Volcanic Group (may be typo?). Geological Province: Georgetown Region.||||||08-JUL-15
23889|Paddock Creek Formation|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V36. I-Type.||||||
23889|Paddock Creek Formation|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23889|Paddock Creek Formation|40542|6|Mentioned|p97|||||||||
23889|Paddock Creek Formation|43259|4|Described|Appendix 1,p4.||Carboniferous|||||||
23889|Paddock Creek Formation|43286|5|Briefly described|Map Legend||Carboniferous|||||||
23889|Paddock Creek Formation|43740|3|Fully described|p26|||||||||
23889|Paddock Creek Formation|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of Bagstowe Ring Structure||||||08-NOV-04
23889|Paddock Creek Formation|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Part of Bagstowe Ring Structure.||||||08-NOV-04
23889|Paddock Creek Formation|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Bagstowe Ring Structure, Kennedy Province. The three facies are mapped separately.|||||Crystal-rich rhyolitic ignimbrite with lithic clasts; rhyolitic volcanic arenite to very coarse volcanic rudite, minor rhyolite; dacitic ignimbrite with chlorite, biotite and lithic clasts and polymictic volcanic rudite with common granitoid clasts.|
23889|Paddock Creek Formation|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bagstowe Ring Structure.|||||Grey to greenish-grey, moderately crystal-rich dacitic ignimbrite with chlorite, biotite and lithic clasts; granule to boulder, polymictic volcanic rudite with common granitoid clasts.|
23889|Paddock Creek Formation|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites, are all mapped under the symbol, Cvk.||||||
23889|Paddock Creek Formation|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned.|||||Rhyolitic ignimbrites, rhyolitic-dacitic lavas and tuff; mostly minor to rare basalt and andesite.|
82624|Palgrave Monzogranite|71628|3|Fully described|p19: 58-60, 65-67, 70-72|||New name (this study). Originally Palgrave Granite of Donchak et al. (2007). Previously part of Herries Monzogranite of Brown et al. (2001, 2007). Named after a local homestead, or the parish or locality of that name. Occurs 27 km SW of Warwick. Forms a 15 x 6 km, N-S trending recessive intrusion cropping out as scattered boulders and low pavements. The type locality is MGA 384034 6854083 (Donchak et al., 2007). Geochemistry described; is assigned to Herries Suite.|256 +/- 1.8 Ma (SHRIMP: Donchak et al., 2007).|Granite Hills Complex.||Intrudes Texas beds. Abuts Fairleigh Monzogranite. Is intruded by Stanthorpe Monzogranite.|Pale grey to pinkish grey, medium- to fine-grained, moderately porphyritic hornblende-biotite monzogranite. I-type.|
25377|Pall Mall Granite|23422|5|Briefly described|p193, p213 Table 6.12|Early Permian|Early Permian|Of Leichhardt Supersuite.  K-Ar age 286 +/- 9 Ma||||||19-OCT-12
25377|Pall Mall Granite|23430|5|Briefly described|p506|||K-Ar age 289 Ma.||||||
25377|Pall Mall Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
25377|Pall Mall Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 83. I-Type.||||||
25377|Pall Mall Granite|42407|6|Mentioned|p22|||Variation of Pall Mall Adamellite?||||||
25377|Pall Mall Granite|42689|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
25377|Pall Mall Granite|43095|2|Defined|p82|Early Permian|Late Carboniferous|K-Ar biotite age of 289 Ma.||||||
25377|Pall Mall Granite|43259|4|Described|Appendix 1,p21.|Early Permian|Late Carboniferous|K-Ar biotite age 289 Ma.||||||
25377|Pall Mall Granite|43589|2|Defined|p24|Early Permian|Late Carboniferous|Superseded Pall Mall Adamellite.  Intrudes Argentine Metamorphics and rocks of the Dotswood Group, and the Ravenswood Granodiorite Complex.||||||23-APR-08
25377|Pall Mall Granite|43933|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
25377|Pall Mall Granite|68419|5|Briefly described|Map Legend|Permian|Permian|Of the Kennedy Province. Shown as Early Permian age.|||||Pink to grey, medium to coarse-grained, porphyritic biotite granite.|
25377|Pall Mall Granite|68420|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Kennedy Province.|||||Pink to grey, medium to coarse-grained, porphyritic biotite granite.|
25377|Pall Mall Granite|68731|6|Mentioned|p188|Cisuralian|Cisuralian||286 +/- 9 Ma|||||
25377|Pall Mall Granite|69593|5|Briefly described|p494, p513|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. Sm-Nd isotope data tabulated.|~310-283 Ma.|Leichhardt Supersuite.|||Hornblende-biotite and biotite granite and granodiorite. I-type.|
39646|Pallamana Sandstone|60659|4|Described|p12, p50 Fig. 2|Early Carboniferous|Late Devonian|Fluviatile sst informally referred to as Molly Darling Sandstone by geologists at local Pajingo mine. Unconformably overlies Rollston Range Fm; conformably overlain; Vera-Nancy Volcanics. Geol Prov: Drummond Basin. See also p51 Fig. 3.||||||07-FEB-11
39646|Pallamana Sandstone|62074|5|Briefly described|p3|Late Devonian|Late Devonian|These rocks had been incorrectly placed in the Raymond Sandstone. Mis-spelt as Palamana. Fossil plants indicate a Late Devonian age.||||Is overlain by Vera Nancy Volcanics.|Quartzo-feldspathic clastic sedimentary rocks.|
39646|Pallamana Sandstone|64850|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Medium- to coarse-grained, cross-bedded quartzose to sublabile sandstone, minor siltstone.||||||
39646|Pallamana Sandstone|64852|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Medium- to coarse-grained, cross-bedded quartzose to sublabile sandstone, minor siltstone.||||||
39646|Pallamana Sandstone|68731|5|Briefly described|p193|Mississippian|Late Devonian|Age constrained on the basis of macroflora (S McLoughlin pers. Comm. 2003). Previously the Molly Darling Sandstone (Patterson and Keys 2003).||||Overlain by the Vera-Nancy Volcanics.|Comprises dominantly medium-grained, cross-laminated sandstone and pebbly sandstone (largely derived from basement sources with a minor volcanogenic component), but locally siltstone may be abundant.|
39646|Pallamana Sandstone|68900|2|Defined|p1, p13, p37-p40|Late Devonian|Late Devonian|Drummond Basin. Occurs in the northern part of HARVEST HOME 1:100k and extends westward into PAJINGO. Originally mapped as Raymond Sandstone on Charters Towers 1:250k sheet. Informally referred to as the "Molly Darling Sandstone" in exploration reports (e.g. Patterson & Keys, 2003). Named for the Pallamana homestead at GR 450845 7730462 in HARVEST HOME. This unit generally produces hilly, darkly vegetated topography.A type area is proposed between GR 442700 773100 and GR 443000 773200. This unit displays weak enrichment in potassium in airborne radiometric images and correlates with magnetic lows in airborne magnetic images. Common lycopod fossils suggest a terrestrial environment, whilst cross-bedded sandstone over siltstone suggests a low sinuosity fluvial system.||||Unconformably overlies the Seventy Mile Range Group, Trooper Creek Formation and the Rollston Range Formation. Overlain by the Vera-Nancy Volcanics (probably conformably).|Quartz-rich, medium-grained, medium-thick bedded sandstones with local siltstones.|
36419|Palm Islands Granite|23617|4|Described|p31|Early Permian|Late Carboniferous|Also see Table 2 p18. Name applied to granite that outcrops on Great Palm Island and other smaller islands. Table 3 p52. Kennedy Province.||||||
36419|Palm Islands Granite|23618|5|Briefly described|map legend||Early Permian|||||||
35186|Palms Lookout Granodiorite|23042|4|Described|p91||Carboniferous|Intruded by Morugo Granite.||||||
35186|Palms Lookout Granodiorite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35186|Palms Lookout Granodiorite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Commonly altered, greenish grey, fine- to coarse-grained hornblende granodiorite to tonalite; pink to cream biotite granite; local pegamtite and aplite and fine-gr. diorite with grandiorite xenoliths; andesite and rhyolite. Part of the Urannah Batholith.||||||25-MAY-06
35186|Palms Lookout Granodiorite|65388|2|Defined|p377-379, p135, p362, 364, 365, 380|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith.  Intruded by Finch Hatton Granite, Morugo Granite. Probable age given. Mainly grey, fine to medium-grained, equigranular biotite-hornblende granodiorite containing diorite, microdiorite xenoliths.||||||
35186|Palms Lookout Granodiorite|73037|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Commonly altered, greenish-grey, fine to coarse-grained hornblende granodiorite to tonalite; pink to cream biotite granite; local pegmatite and aplite and fine-grained diorite with granodiorite xenoliths; andesite and rhyolite dykes.|
23891|Paluma Rhyolite|23422|5|Briefly described|p181, p205 Table 6.3|Visean|Visean|||||||
23891|Paluma Rhyolite|23430|6|Mentioned|p489|||||||||
23891|Paluma Rhyolite|23431|5|Briefly described|p538|||||||||
23891|Paluma Rhyolite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23891|Paluma Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V52. I-Type.||||||
23891|Paluma Rhyolite|23617|4|Described|p14|Permian|Carboniferous|Intruded by Rollingstone Granite and Coane Range Granite Complex. Kennedy Province.||||||
23891|Paluma Rhyolite|23618|5|Briefly described|map legend||Carboniferous|||||||
23891|Paluma Rhyolite|23893|5|Briefly described|p18|Visean|Visean|Of Oweenee Supersuite.  Geological Province: Kennedy Province.||||||
23891|Paluma Rhyolite|24613|5|Briefly described|p113, p114|Early Carboniferous|Early Carboniferous|||||||07-FEB-11
23891|Paluma Rhyolite|42689|5|Briefly described|map legend|Carboniferous||||||||
23891|Paluma Rhyolite|43095|2|Defined|p31|Early Carboniferous||||||||
23891|Paluma Rhyolite|43106|5|Briefly described|p27|||||||||
23891|Paluma Rhyolite|43259|4|Described|Appendix 1,p5.||Early Carboniferous|||||||
23891|Paluma Rhyolite|43589|2|Defined|p20|Early Carboniferous|Early Carboniferous|Unconformably overlies Saint Giles Volcanics. Intruded by Coane Range Granite Complex in west, and by Clemant Microgranite in east.||||||19-JUN-13
23891|Paluma Rhyolite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Is intruded by the Coane Range Granite Complex and Clemant Microgranite.|Dark grey, crystal-rich to very crystal rich rhyolitic ignimbrite.|
23891|Paluma Rhyolite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Is intruded by Coane Range Granite Complex and Clemant Microgranite.|Dark grey, crystal-rich to very crystal-rich rhyolitic ignimbrite.|
23891|Paluma Rhyolite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
23891|Paluma Rhyolite|69593|5|Briefly described|p494-496|Visean|Visean|Forms scattered outcrops in the Townsville region. May be included in the Oweenee Supersuite.|||||Thick sheets of crystal-rich to lithic-rich rhyolitic to dacitic ignimbrite; minor tuff, lava, breccia.|
36489|Pamplemousse complex|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 72.  I-Type.||||||
77885|Pandanus Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Purplish brown and grey thin-bedded and laminated micaceous siltstone, shale and fine sandstone.|
77885|Pandanus Formation|68146|5|Briefly described|p21|||||Wild Cow Subgroup.||Is overlain by Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77885|Pandanus Formation|68575|5|Briefly described|p19|||South Nicholson Basin.||Wild Cow Subgroup.||Is overlain by Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77885|Pandanus Formation|69591|5|Briefly described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Storm-dominated shelf deposits.||Wild Cow Subgroup.||Overlies Hedley Sandstone. Is overlain by Burangoo Sandstone.|Purplish-brown and grey, thin-bedded and laminated micaceous siltstone, shale and fine sandstone.|
77885|Pandanus Formation|71369|4|Described|p1, p6, p8-9, p11-15, p22, p35, p47, p49|Mesoproterozoic|Mesoproterozoic|See also p19. South Nicholson Basin. Previously the Pandanus Siltstone Member (Smith and Roberts, 1962; Roberts et al., 1963) of Constance Sandstone. Raised to Formation status in this study (Sweet, 2017). Rarely exposed; covered by debris on scree slopes. Up to 130m thick. Shallow- to moderate-depth shelf deposits. Outcrop pattern indicates left lateral (fault) movement of 700-800m.|c.1500 Ma.|Wild Cow Subgroup.||Overlies Hedleys Sandstone. Is overlain by Burangoo Sandstone ?unconformably.|Greyish-green to greyish red shale coarsening-up to siltstone and interbedded fine-grained sandstone.|20-FEB-18
77885|Pandanus Formation|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|26-NOV-19
77885|Pandanus Formation|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Burangoo Sandstone. Underlain by Hedleys Sandstone.|Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Burangoo Sandstone. Underlain by Hedleys Sandstone.|Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus Formation|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||South Nicholson Group||Overlies Hedleys Sandstone and underlies Burangoo Sandstone.||
77885|Pandanus Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Hedleys Sandstone and underlies Burangoo Sandstone.|Includes siltstone.|
77885|Pandanus Formation|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Hedleys Sandstone and underlies Bunangoo Sandstone.|Includes siltstone.|
77885|Pandanus Formation|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in Qld. Distinct from Pandanus Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77885|Pandanus Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Hedleys Sandstone. Overlain by Burangoo Sandstone.||
77885|Pandanus Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Hedleys Sandstone. Overlain by Burangoo Sandstone.||
28201|Pandanus Siltstone Member|23065|6|Mentioned|17|||Geological province: South Nicholson Basin. Of the South Nicholson Group.||||||22-NOV-06
28201|Pandanus Siltstone Member|23393|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|Of Constance Sandstone.||||||
28201|Pandanus Siltstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Constance Sandstone.||||||
28201|Pandanus Siltstone Member|35640|6|Mentioned|Map legend|Adelaidean|Carpentarian|Prob. Adelaidean - Carpentarian.||||||22-NOV-06
28201|Pandanus Siltstone Member|36012|3|Fully described|Table 4|||||||||
28201|Pandanus Siltstone Member|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||22-NOV-06
28201|Pandanus Siltstone Member|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||22-NOV-06
28201|Pandanus Siltstone Member|38584|4|Described|p19|||||||||
28201|Pandanus Siltstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
28201|Pandanus Siltstone Member|41721|4|Described|p29|||Of Constance Sandstone. Thickness: 130m. Fissile/ flaggy, green, purplish-brown and grey coarse siltstone with shaly partings and thin interbeds of very fine to fine-grained sandstone and wacke; middle section often contains a prominent bed of blocky sst.||||||02-AUG-07
28201|Pandanus Siltstone Member|44305|14|Not recorded|p.14-15||Neoproterozoic|Defn. on Tech.File (E/53-8). opp.6. U.Prot.||||||
28201|Pandanus Siltstone Member|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
28201|Pandanus Siltstone Member|44482|14|Not recorded|p.9,opp. p.6, map|||(E53-12). (Of Constance Sandstone).||||||
28201|Pandanus Siltstone Member|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
28201|Pandanus Siltstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Constance Sandstone.||||||
28201|Pandanus Siltstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Constance Sandstone. Flaggy brown micaceous lithic fine grained sandstone; minor siltstone and shale.||||||
28201|Pandanus Siltstone Member|65337|3|Fully described|p9 Fig.5, p38 Table 5, p51.|Mesoproterozoic|Mesoproterozoic|Deeper marine: lower shoreface and shelf environment. Shows parting lineations, hummocky cross-stratification, small trough cross-beds, parallel lamination, slumping and convolute bedding.||Unit in Constance Sandstone.||Overlies Hedleys Sandstone Member. Is overlain by Burangoo Sandstone Member.|Flaggy, brown, micaceous, lithic fine-grained sandstone; minor siltstone and shale.|
28201|Pandanus Siltstone Member|67539|6|Mentioned|p15 Fig.8|||Replaced by Pandanus Siltstone||||||
28201|Pandanus Siltstone Member|69434|4|Described|p19:2, 6|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. 20-50m thick. Deeper-marine deposits: lower shoreface and storm-dominated shelf.||Constance Sandstone.||Conformably overlies Hedleys Sandstone Member. Is overlain conformably by Burangoo Sandstone Member.|Flaggy, micaceous, lithic fine sandstone; minor siltstone and shale.|12-JUL-16
28201|Pandanus Siltstone Member|70897|5|Briefly described|p38, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|Represents regional flooding episodes.||Constance Sandstone.|||Siltstone, shale.|
28201|Pandanus Siltstone Member|71369|5|Briefly described|p5-6, p8, p13, p20|Mesoproterozoic|Mesoproterozoic|Smith and Roberts (1962), Roberts et al. (1963) as a unit in Constance Sandstone. Raised to Formation status in this study (Sweet, 2017). South Nicholson Basin. Misnamed in Fig.2d on p6 as Pandanus Sdst Mbr.||Constance Sandstone||||20-FEB-18
28201|Pandanus Siltstone Member|72526|5|Briefly described|p33,|||Of Rawlings et al. (2008) [Name replaced by Pandanus Formation].||Of Constance Sandstone of Rawlings et al., 2008.||||
28201|Pandanus Siltstone Member|72527|6|Mentioned|p7 Fig.1.4, p41.|Mesoproterozoic|Mesoproterozoic|Shown as (abbreviated) sandstone member on p7 Fig. 1.4.||Constance Sandstone||Overlies Hedley Sandstone Member and underlies Burangoo Sandstone Member.||
28201|Pandanus Siltstone Member|72919|6|Mentioned|p47|Ectasian|Calymmian|Rawlings et al. (2008).||Of Constance Sandstone.||||
75731|Panhandle Granite|70740|5|Briefly described|p126, p127|||Outcrop characteristics and distribution briefly discussed. In contact with a number of units (Lizzie Creek Volcanics, Goldbeetle Creek Granodiorite and Glenella Creek Granite) though relationships aren't given.||||Probably intruded by the Glenmore Creek Granodiorite.|Medium-grained, slightly to moderately porphyritic biotite monzogranite and monzogranite with mafic inclusions, miarolitic cavities and vuggy pegmatitic zones.|
23892|Paning Member|13497|4|Described|iv, vi, viii, xii, p69 fig 6.1|Anisian|Scythian|Cooper Basin.This member was initialtly defined by Powis (1989) however it was subsequently redefined by Channon and Wood (1989). Three reference sections are mentioned, including one from Powis (1989) and two from Channon and Wood (1989). Petrography discussed in detail. Distribution is briefly discussed. More than 200m thick in the Moomba Field where it has been drilled. Outcrop and reservoir characteristics discussed. See also p104-p105, p108-p110, p157 tbl 10.1 , p159, p161, p166, p172.||Arrabury Formation||Disconformably overlies the Callamurra Member. Overlain by and is equivalent to, the Wimma Sandstone Member.|Upwards-fining cycles of buff, pale grey to off white, fine to medium-grained sandstone grading into light to dark grey and brown siliceous mudstone and siltstone.|
23892|Paning Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation||||||
23892|Paning Member|23155|6|Mentioned|Fig 8 on p16|||Age - Triassic?||||||
23892|Paning Member|23375|4|Described|Fig2 p265,280|Nammalian|Griesbachian|Of the Arrabury Formation, Cooper Basin.||||||17-JAN-08
23892|Paning Member|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Early Triassic|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
23892|Paning Member|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
23892|Paning Member|42008|3|Fully described|PP270|Scythian|Tatarian|Of the Arrabury Formation.||||||17-JAN-08
23892|Paning Member|42085|6|Mentioned|Fig.2 P374|||||||||
23892|Paning Member|44133|5|Briefly described|p65 Fig. 8.3, 86|Triassic|Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin. Overlies: Callamurra Member (u).||||||
23892|Paning Member|60717|5|Briefly described|p40 Fig. 2|Scythian|Scythian|Of Arrabury Formation (Nappamerri Group). Overlies Callamurra Member and part of Paning Member of the same unit. Thickness: 150m. Geological Province: Cooper Basin.||||||31-JAN-08
23892|Paning Member|61613|5|Briefly described|p282 Fig. 2|Early Triassic|Late Permian|Of Arrabury Formation. Overlain by Wimma Sandstone Member, Underlain by Callamurra Member. Geological Province: Cooper and Simpson Basins.||||||26-JUN-14
23892|Paning Member|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
23892|Paning Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Arrabury Formation. Geological Province: Cooper Basin.||||||31-MAR-09
23892|Paning Member|62730|5|Briefly described|p352 Fig. 1|Early Triassic|Early Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
23892|Paning Member|63978|2|Defined|p21, Fig. 3|Early Triassic|Early Triassic|Of Arrabury Fm. Paning Mbr originally included Callamurra Mbr also (Powis 1989); then redefined by Gary (2000) interpreting the Callamurra Mbr conformably below Paning Mbr. Conformable below Wimma Sst Mbr. Max. thick: 200m. Detailed lithology included.||||||07-FEB-11
23892|Paning Member|64048|5|Briefly described|p66|||Within the Middle Arrabury Formation. Directly overlies the Callamurra Member. Contains considerable amounts of interbedded sandstones which contain commercial quantities of gas.||||||07-FEB-11
23892|Paning Member|64197|6|Mentioned|p625 Fig.1c|Early Triassic|Early Triassic|Cooper Basin||Unit in Arrabury Formation||Overlies Callamurra Member. Is overlain by Wimma [Sandstone] Member.||
23892|Paning Member|64665|5|Briefly described|p53 Fig.2.|Early Triassic|Early Triassic|Cooper Basin.||Middle unit in Arrabury Formation.||Is overlain by Wimma Sandstone Member.||
23892|Paning Member|65489|5|Briefly described|p48, p96, p131-132|Scythian|Scythian|150m thick. Hosts economic oil and gas reservoirs.||Unit in Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|67402|5|Briefly described|p90 fig CPR4|||Misspelt as the Panning Member on p91. Probably a facies equivalent of the Wimma Sandstone Member. Maximum thickness of 150m. See also p91 tbl CPR1, p90-p94, p101, p101 tbl CPR2, p105.||Arrabury Formation||Conformably (or mildly unconformably) overlies the Callamurra Member. Conformably overlain by the Wimma Sandstone Member.|Fine to medium-grained sandstones and siltstones that fine upwards.|
23892|Paning Member|68731|5|Briefly described|p200 Fig 3.110, p207|Middle Triassic|Early Triassic|Cooper Basin. Strata that Powis (1989) assigned to the lower Paning Member is now included in the Callamurra Member.||Of the Arrabury Formation.||Underlain by the Callamurra Member (possible disconformity). Conformably overlain by the Wimma Sandstone Member.||
23892|Paning Member|69797|5|Briefly described|p17 Fig.2|Early Triassic|Early Triassic|Age: Scythian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
23892|Paning Member|69946|5|Briefly described|p9, p36, p54|Scythian|Scythian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||||
23892|Paning Member|70317|6|Mentioned|p33|Early Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||Overlies Callamurra Member. Is overlain by Wimma Sandstone Member.||
23892|Paning Member|70823|5|Briefly described|p40, p75, p79, p81|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlain by the Wimma Sandstone Member.|Thin fine to medium grained quartzose sandstones.|
23892|Paning Member|70824|4|Described|p7, p104|Olenekian|Olenekian|Cooper Basin. Deposited in braided fluvial channels and floodplain environments.||Arrabury Formation||Unconformably overlies the Callamurra Member. Conformably overlain by the Wimma Sandstone Member.|Basal mudstone and siltstone with thin fine to medium-grained quartzose sandstone interbeds.|
23892|Paning Member|70946|5|Briefly described|p1089|Early Triassic|Early Triassic|Cooper Basin. Deposited in a braided fluvial channel belt and floodplain environment.||Arrabury Formation.||Unconformably overlies the Callamurra Member.||08-OCT-18
23892|Paning Member|71265|5|Briefly described|p589|Olenekian|Olenekian|Cooper Basin.||Arrabury Formation.||Overlies Callamurra Member.||
23892|Paning Member|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54, Ch7 p13|Anisian|Scythian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial channel or floodplain environment.||Arrabury Formation||Overlies the Callamurra Member. Overlain by the Wimma Sandstone Member.||
23892|Paning Member|71701|5|Briefly described|p155|Olenekian|Olenekian|Cooper Basin.||Arrabury Formation||Unconformably overlies the Callamurra Member.||
23892|Paning Member|73251|6|Mentioned|p62|Early Triassic|Early Triassic|Cooper Basin. Braided fluvial channel belt and floodplain depositional environments. Contains[?] gas and oil.||Arrabury Formation, Nappamerri Group||Underlain by Callamurra Member. Overlain by and equivalent to Wimma Sandstone Member.||
36163|Panorama Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36163|Panorama Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 266. I-Type.||||||
36163|Panorama Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36163|Panorama Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, fine- to medium-grained, (tourmaline-) biotite granite. I-type.||||||07-FEB-11
76893|Paper Tank Microgranite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event.||Kalkadoon Supersuite|||Pink to brown, fine grained, biotite microgranite; locally sparsely finely porphyritic; strong linear fabric; locally strongly foliated.|
76893|Paper Tank Microgranite|68146|5|Briefly described|p194|||Formerly considered part of the Tewinga Group. Coeval with c.1795 Ma Big Toby Granite and other units (listed).|1792 +/- 7 Ma; Magee et al. (in press).|||||
76893|Paper Tank Microgranite|68575|5|Briefly described|p1, p6-7, p82-86, p124, p134|||Mount Isa Region. Crops out 22km SSE of Dajarra. Previously mapped as Argylla Formation by Blake (1987); also as part of the Tewinga Group in the Dajarra 100K sheet. Said to have been mapped as Tewinga Gneiss (p1) without specifying where. May be a subvolcanic intrusive related to the Bottletree Formation which crops out 15km along strike to the north: they are of a similar age. Is older than Argylla Formation and 65 m.y. younger than Tewinga Gneiss, necessitating revision of map units, stratigraphy and nomenclature. Whole rock Sm-Nd isotopic data and age (1792 Ma).|1791 +/- 7 Ma.||||Pink gneissic microgranite.|
76893|Paper Tank Microgranite|69591|5|Briefly described|p60||||1792 +/- 7 Ma (Magee et al., in press).||||Pink to brown, fine-grained biotite microgranite; locally sparsely finely porphyritic; strong linear fabric; locally strongly foliated.|
76893|Paper Tank Microgranite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1791+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
76893|Paper Tank Microgranite|73553|6|Mentioned|p259|Statherian|Statherian|Kalkadoon-Leichhardt Domain.|1791+/-7 Ma (Magee et al., 2012)|||||
36170|Parada Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36170|Parada Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 244. I-Type.||||||
36170|Parada Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36170|Parada Granite|60425|5|Briefly described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. White, fine- to medium-grained, even-grained biotite granite.||||||07-FEB-11
36170|Parada Granite|72983|6|Mentioned|p1, p18|mid-late Carboniferous|mid-late Carboniferous|||||Intruded by Collins Weir Rhyolite.||
36287|Parallel Creek Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Galloway Volcanic Group.||||||
36246|Parker Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36246|Parker Microgranite|60425|5|Briefly described|p282-3 Appdx., p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Topaz-bearing microgranite; included in Go Sam Granite on most recent maps. I-type.||||||07-FEB-11
32136|Parraweena Gabbro|23037|4|Described|p79,80|Permian|Silesian|Intrudes the Glenhalvern Granite, Torsdale Volcanics and the Lonesome Creek Monzonite.||||||
32136|Parraweena Gabbro|24615|5|Briefly described|CD|Permian|Permian|[Pgpw].  Dark grey to black, medium-grained hornblende plagioclase gabbro;  medium to coarse leucograbbro.||||||
32136|Parraweena Gabbro|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Dark grey to black, medium-grained, hornblende plagioclase gabbro; medium- to coarse-grained leucogabbro.||||||18-MAY-04
32136|Parraweena Gabbro|65388|2|Defined|p271, p264, p236 Fig. 81, p237, 238, 325|Early Triassic|Permian|Auburn Arch. Shown as Parrawee Gabbro p253 Fig. 87. Appears to intrude the Torsdale Volcanics, Glenhalvern Granite, and Lonesome Creek Quartz Monzodiorite. Age could be early Permian or late Permian to Early Triassic. Dark grey to black, medium to coarse grained hornblende gabbro. Outcrop very poor.||||||
32136|Parraweena Gabbro|68679|5|Briefly described|p407-408, p419|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Torsdale Volcanics, Glenhalvern Granite and Lonesome Creek Quartz Monzodiorite.|Grey to black, medium- to coarse-grained hornblende gabbro.|
24451|Parrot Camp Rhyolite|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Rhyolitic ignimbrite.  Overlies B Creek Rhyolite; overlain by Carron Rhyolite.||||||24-JUN-04
24451|Parrot Camp Rhyolite|23291|4|Described|p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Croydon Volcanic Group. Thickness: up to 300m? Geological Province: Georgetown Region.||||||08-JUL-15
24451|Parrot Camp Rhyolite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V803. S-Type.||||||
24451|Parrot Camp Rhyolite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24451|Parrot Camp Rhyolite|40659|2|Defined|p252|Mesoproterozoic|Mesoproterozoic|||||||
24451|Parrot Camp Rhyolite|40954|6|Mentioned|p132|||||||||
24451|Parrot Camp Rhyolite|41975|5|Briefly described|Fig.3 P433|||||||||
24451|Parrot Camp Rhyolite|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24451|Parrot Camp Rhyolite|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
24451|Parrot Camp Rhyolite|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24451|Parrot Camp Rhyolite|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|||Greenish-grey to dark grey moderately crystal-rich rhyolitic ignimbrite, similar to Idalia Rhyolite but tends to be darker.|
24451|Parrot Camp Rhyolite|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Conformably overlies B-Creek Rhyolite. Is overlain conformably by Carron Rhyolite.|Greenish-grey to dark grey moderately crystal-rich rhyolitic ignimbrite, similar to Idalia Rhyolite but tends to be darker.|
24451|Parrot Camp Rhyolite|69591|5|Briefly described|p74 Tb.2.5, p75|||Croydon Province, Georgetown Inlier. Up to 300m ? thick. With the Idalia Rhyolite, forms about 80% of the Group's exposed area.||Croydon Volcanic Group.|||Crystal-rich rhyolitic ignimbrite. Intensely welded, extensively recrystallised, crystal-rich and pumice-poor; eutaxitic textures are absent or very obscure.|
72487|Passage Islet Granite|68679|5|Briefly described|p360-361, p367-368, p433|Late Triassic|Early Triassic|The formal name appears on Figs 5.58, 5.61 and in the Index; in the text the unit appears as Passage Islet granite or, more commonly, as "Gloucester and Passage Islet granites". Geochemical described, with plots. Described as Early Triassic p367, 368, but K-Ar age of 224 Ma and 221 Ma (p433) are both Late Triassic, and described as such on p433.|||||Biotite granite. Mainly I-type.|28-MAY-20
72487|Passage Islet Granite|68901|6|Mentioned|p110|||Exposed on Passage Islet. Is closely associated with and genetically related to the Gloucester Granite (magmatic crystallisation age 243.6+/-2 Ma).||||||28-MAY-20
72487|Passage Islet Granite|69594|6|Mentioned|p571 Fig.7.45|||Geochemistry plot and discussion.||||||
82415|Passchendaele Monzogranite|71628|5|Briefly described|p12: 1, 9-11, 17; p15: 33, 43, 82|||New name, from the locality of Passchendaele. Crops out ~17 km NW of Stanthorpe. Limited geochemistry described.||Sailor Jack Suite, Sailor Jack Supersuite.||Is faulted against the Texas beds. Is partially enclosed (intruded) by the younger Amiens Leucomonzogranite and Ruby Creek Leucogranite (Stanthorpe Complex).|Pale grey, medium-grained, weakly porphyritic biotite-hornblende monzogranite; cut by aplitic dykes. I-type.|
77805|Pat and Peter Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Biotite granite and porphyritic biotite microgranite; hydrothermally altered biotite granite, porphyritic biotite microgranite.|
36322|Patrick Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Featherbed Volcanic Group.||||||
36322|Patrick Rhyolite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||31-MAY-04
36322|Patrick Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Three facies are mapped separately.||Unit in Featherbed Volcanic Group.|||Pale brown to white, slightly porphyritic rhyolitic lava; flow-banded in places; pale, devitrified crystal-poor rhyolitic ignimbrite; pale, poorly-welded, rhyolitic ignimbrite, rhyolitic lava, and fine ash vitric tuff.|
36288|Paulet Dacite|23291|4|Described|p93 Table 3.9|Early Permian|Early Permian|Parent: Galloway Volcanic Group. Age: 290+3Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36288|Paulet Dacite|23510|5|Briefly described|Map Legend||Early Permian|of Galloway Volcanic Group.||||||
77686|Paynes Lagoon Amphibolite|68350|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.||Unit in Argentine Metamorphics.||Conformably overlies Brinagee Schist.|Laminated amphibolite, quartzite, banded-iron-formation, subordinate mica schist.|
77686|Paynes Lagoon Amphibolite|68351|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.||Unit in Argentine Metamorphics.||Conformably overlies Brinagee Schist.|Laminated amphibolite, quartzite, banded-iron-formation, subordinate mica schist.|
77686|Paynes Lagoon Amphibolite|68419|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Cape River Province. Minimum age shown as possibly Ordovician.||Of the Argentine Metamorphics.||Conformably underlain by the Brinagee Schist.|Laminated amphibolite, quartzite, banded-iron-formation, subordinate mica schist.|
77686|Paynes Lagoon Amphibolite|68420|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Cape River Province. Minimum age shown as possibly Ordovician.||Of the Argentine Metamorphics.||Conformably underlain by the Brinagee Schist.|Laminated amphibolite, quartzite, banded-iron-formation, subordinate mica schist.|
36498|Peach Hollow Knobs rhyolite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 130.||||||
30894|Peak John Well Granite|22675|4|Described|p158 App.1|||||||||
30894|Peak John Well Granite|43391|5|Briefly described|Map legend|Permian|Carboniferous|Carboniferous and/or Permian.  Biotite granite and granodiorite.||||||23-JUN-04
30894|Peak John Well Granite|60659|5|Briefly described|p18|||Pale grey to pale pink and locally white to cream, very fine- to coarse-grained biotite granite and subsidiary granodiorite. Age: 324+/-3Ma (Rb-Sr biotite) and 328+/-3Ma (Rb-Sr whole rock).||||||07-FEB-11
30894|Peak John Well Granite|68900|6|Mentioned|p18|||||||Intrudes the Les Jumelles beds.||
30894|Peak John Well Granite|69593|5|Briefly described|p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.||||I-type.|
30894|Peak John Well Granite|70740|5|Briefly described|p20, p127, p128|Permian|Carboniferous|Appears to be intruded by the Mount Magnus Granite. Outcrop distribution and geophysical (magnetic) characteristics briefly mentioned. |328 +/- 3 Ma (Rb-Sr Oversby et al., 1994)|||Intrudes the Les Jumelles beds and the Ukalunda Formation.|Fine-grained, moderately to highly porphyritic, leucocratic biotite monzogranite with traces of allanite, fluorite and scarce mafic inclusions.|
23894|Peak Vale Granodiorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1||||||
23894|Peak Vale Granodiorite|43029|2|Defined|p19||Middle Devonian|Rb-Sr dating of 369 Ma and 376 Ma. See also Fig.2,p16||||||
23894|Peak Vale Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
23894|Peak Vale Granodiorite|43213|3|Fully described|p96-97, p107, p116-121, p174-175, p177|Middle Devonian|Middle Devonian|See also p208, p211, p222, p232, p240, p242. Type locality described. Component of the Retreat Batholith. Could belong to either Mount Newsome or Kilmarnock Suites. Rb-Sr biotite-whole rock pair ages (Carr, pers. Comm., 1993) from the granodiorite and quartz monzonite respectively. Geochemistry, modal and chemical analyses and geophysics detailed. Appears as Peak Vale Granite on p174.|369 +/- 3 Ma and 376 +/- 3 Ma.|||Intrudes Anakie Metamorphic Group and (probably) the Kilmarnock Granodiorite.|Two main rock types: grey, fine- to coarse-grained, subequigranular to porphyritic pyroxene-biotite-hornblende granodiorite; and subordinate biotite-hornblende quartz monzodiorite of similar texture.|
23894|Peak Vale Granodiorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey, fine to coarse-grained, subequigranular to porphyritic pyroxene-biotite-hornblende granodiorite and subordinate quartz monzodiorite.|
24619|Peera Peera Formation|13497|5|Briefly described|p65, p114|||Simpson Basin. Up to 190m thick.||||Equivalent to the Cuddapan Formation.||
24619|Peera Peera Formation|22839|6|Mentioned|P33|||Lateral equivalent of the Cuddapan Formation||||||
24619|Peera Peera Formation|22857|5|Briefly described|p310|Late Triassic|Late Triassic|Geological Province: Eromanga Basin.||||||
24619|Peera Peera Formation|22865|6|Mentioned|p310||Late Triassic|||||||
24619|Peera Peera Formation|22883|5|Briefly described|P31, Fig2||Late Triassic|Correlated to the Cuddapan Formation, underlying unit is Walkandi Formation.||||||16-SEP-08
24619|Peera Peera Formation|24204|5|Briefly described|p262, 263 Fig.4|Late Triassic|Late Triassic|Shale, coal, sandstone. Overlies Walkandi Formation (unconformable). Geological Province: Simpson Basin.||||||
24619|Peera Peera Formation|36922|6|Mentioned|Fig.3|||Note with Fig.4 states name should be P.P.beds. Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|36941|6|Mentioned|Table 1|||||||||
24619|Peera Peera Formation|37287|6|Mentioned|p36|||||||||
24619|Peera Peera Formation|37776|6|Mentioned|Fig.2|||||||||
24619|Peera Peera Formation|38108|6|Mentioned|Table 1|||Misspelling of Peera Perra?||||||
24619|Peera Peera Formation|41063|2|Defined|p45|Late Triassic|Late Triassic|||||||
24619|Peera Peera Formation|41099|6|Mentioned|Fig.9|||||||||
24619|Peera Peera Formation|41176|6|Mentioned|p206|||||||||
24619|Peera Peera Formation|41183|6|Mentioned|p310|||||||||
24619|Peera Peera Formation|42008|5|Briefly described|p265,266, 267, 268, 275|Late Triassic|Late Triassic|Simpson Desert Basin. Correlated with Cuddapan Formation. Also shown as Peera Perra Formation on p266.||||||09-APR-15
24619|Peera Peera Formation|42062|5|Briefly described|p27|||||||||
24619|Peera Peera Formation|42463|6|Mentioned|Fig.4 P171|||||||||
24619|Peera Peera Formation|42746|4|Described|p6, Fig.2 p4|||||||||
24619|Peera Peera Formation|43052|5|Briefly described|Table 2.1|||||||||
24619|Peera Peera Formation|44133|5|Briefly described|p94|Late Triassic|Late Triassic|Conformably overlies: Walkandi Formation. Maximum Thickness: 190m. ||||||
24619|Peera Peera Formation|62376|5|Briefly described|p84|Late Triassic|Middle Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
24619|Peera Peera Formation|63979|6|Mentioned|p31|||Geological province: Simpson Basin. Correlate of Cuddapan Formation.||||||07-FEB-11
24619|Peera Peera Formation|64778|6|Mentioned|p13, 28|Triassic|Triassic|Simpson Desert Basin. Potential hydrocarbon source.||||||
24619|Peera Peera Formation|65238|5|Briefly described|p7 Fig. 8, p9|Late Triassic|Middle Triassic|Unconformably overlies Walkandi Formation. Max. thickness: 200m. Geological province: Simpson Desert Basin. Lacustrine, low energy, meandering deposits comprising thick, broadly upward-fining succession. Very detailed lithology included. See also p10.||||||
24619|Peera Peera Formation|65489|5|Briefly described|p53, p55-63, p137, p149-151|Late Triassic|Middle Triassic|Simpson Basin. 190m thick. Hydrocarbon source rock; hosts oil show and gas indication. Poor quality reservoirs; intrafomational siltstone and shale form seals.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation (Cooper Basin). Probably correlates with Tinchoo Formation.|Basal grey shale and siltstone with minor thin sandstone and coal, a fining upward sandy middle unit, and black highly carbonaceous silty shale at the top.|
24619|Peera Peera Formation|69454|5|Briefly described|p38:3-4, 8-13, 14 Fig.38.9|Rhaetian|Carnian|Pedirka Basin (subsurface only). 190m thick in Walkandi-1. Meandering fluvial, lacustrine/paludal deposits. May be equivalent to uppermost part of the Tinchoo Formation. Hosts minor coal resources with fair to good mixed oil-gas source potential. Sandstones have fair to good reservoir potential, with intra-formational shale seals.||||Overlies Purni Formation unconformably, and Walkandi Formation disconformably or unconformably. Is overlain unconformably by Poolowanna Formation. Correlated with Cuddapan Formation (Eromanga Basin).|Shale, siltstone, minor coal and sandstone at base, overlain by cyclical upward-fining sandstone, capped by highly carbonaceous shale with occasional thin sandstone beds.|12-JUL-16
24619|Peera Peera Formation|69457|6|Mentioned|p41:5 Fig.41.4; 41:16|Triassic|Triassic|Fair to good source rocks.||||||12-JUL-16
24619|Peera Peera Formation|69673|5|Briefly described|p152, 159, 160, 161, 149|Triassic|Triassic|190m thick. Source rock potential.||||Unconformably overlies Purni Formation, unconformably overlain by Poolowanna Formation|Shale, siltstone, minor sandstone and coal. Black silty and highly carbonaceous shale with occasional thin sandstone interbeds.|21-SEP-17
24619|Peera Peera Formation|69946|4|Described|p8-9, p36, p51-52|Late Triassic|Late Triassic|Defined by Moore (1986); previously Peera Peera beds of Wiltshire (1978). Type section is the interval 2593 - 2768m in Poolowanna 1. Up to 190m thick. Simpson Basin.||||Conformably overlies Walkandi Formation. Correlated with Cuddapan Formation.|Lowermost (of three) units is siltstone and shale with minor thin sandstone and rare coal; then upward-fining sandstone cycles; topped by black carbonaceous shale, coal and thin sandstone interbeds.|
24619|Peera Peera Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Walkandi Formation conformably and Purni Formation unconformably. Is overlain unconformably by Poolowanna Formation.||
24619|Peera Peera Formation|71321|6|Mentioned|p15|||Of Simpson Basin.||||Overlies the Walkandi Formation. Overlain by the Poolowanna Formation.||24-OCT-19
24619|Peera Peera Formation|71342|4|Described|Ch4 p25, Ch5 p8-p9|Triassic|Triassic|Simpson Basin. Originally the informal Peera Peera beds of Wiltshire (1978) before being defined by Moore (1986). A type section in Poolowanna 1 is mentioned. This unit was subdivided into three facies by Moore in 1986. A maximum thickness of 190m is recorded in Walkandi 1. Deposited in a high-sinuosity fluvial environment. See also Ch5 p30, Ch5 p36, Ch5 p51-p52, Ch9 p18, Ch11 p6, Ch12 p2-p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p10-p14, Ch14 p4-p7.||||Conformably overlies the Walkandi Formation. Overlain by the Poolowanna Formation.|Siltstone and shale, minor thin sandstone and rare coal. Black carbonaceous shale, coal and thin sandstone interbeds also occurs.|
24619|Peera Peera Formation|72476|6|Mentioned|p36 Fig.9, p37|Triassic|Triassic|Simpson Basin. Time-temperature thermal history diagram. Only 200m thickness preserved.||||||
24619|Peera Peera Formation|73281|6|Mentioned|p1, Appendix (DIP)|Triassic|Triassic|Pedirka Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
83679|Pegasus Seam|73305|6|Mentioned|p551, p552 Fig.4, p554-556, p560|Late Permian|Late Permian|Bowen Basin. Second-order coal seam within the Fair Hill Formation split from the FH1 seam [Fair Hill Seam]. 1.5 to 11.3 m thick. See also p555 Fig.7, p556 Fig.8.||Fair Hill Formation|||Coal seam.|12-FEB-23
22637|Pelican Creek Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group||||||
22637|Pelican Creek Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p35|||Intrudes Dinah Formation and Sugarbag Creek Quartzite. Grey, fine-grained, equigranular to sparsely porphyritic muscovite-biotite granite.||||||27-JAN-09
22637|Pelican Creek Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
79130|Pengelly Siltstone Member|70913|4|Described|p27-29, p2, 10, p8 fig 3, App 1 maps|Middle Permian|Sakmarian|Gympie Province. Named for the Pengelly Bridge. Previously 'Phoenix slates', 'Monkland slates', Pengelly Siltstone. Revised herein to Member of the Rammutt Formation, but see also previous name Pengelly Siltstone (p7, 8, 10, 12, 87,98) and abbreviation p24, p 67 Fig 9, p75, 76, 79.Reference drill holes mentioned. Hosts a swarm of narrow veins which yield rich gold where they intersect carbonaceous beds. Most economically important unit on the Gympie Goldfield. Distribution and fossil assemblage discussed. Maximum thickness between 70-80m. See also Pengelly Sitlstone member p2.||Rammutt Formation||Overlies the Nash Clastics Member. Overlain by the Glanmire Conglomerate Member or Langton Dolerite.|Dark grey carbonaceous siltstone and shale. Fossiliferous in parts.|19-SEP-17
22638|Penny Gneiss|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Newberry Metamorphic Group||||||12-JAN-05
22638|Penny Gneiss|22781|4|Described|p16|Proterozoic|Proterozoic|Newberry Metamorphic Group||||||
22638|Penny Gneiss|23420|5|Briefly described|p 144 table 4.4|Calymmian|Statherian|In the Newberry Metamorphic Group. Age:1561+/- Ma, 1638 +/-9 Ma||||||
22638|Penny Gneiss|43596|5|Briefly described|p14-15, p20 Tb. 1||Proterozoic|Of Newberry Metamorphic Group.  Typical lithologies are: medium- to coarse-grained, grey, muscovite-biotite-feldspar gneiss and saccharoidal quartzite, associated with pegmatititc leucosome "sweats" and interlayered granite.||||||27-JAN-09
22638|Penny Gneiss|43738|6|Mentioned|p56|||||||||
22638|Penny Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Newberry Metamorphic Group||||||24-JAN-05
22638|Penny Gneiss|69591|5|Briefly described|p73 Tb.2.4|Paleoproterozoic|Paleoproterozoic|Over 400 km2 N of Mount Newberry (exposed mostly along Little Stewart River); small exposures around the Morehead River. Thickness, boundary relationships and relative age are unknown. The ~1561 Ma rims have grown on 1638 +/- 9 Ma inherited cores.|1561 +/- 15 Ma (igneous zircon rims).|Newberry Metamorphic Group.|||Muscovite-biotite-feldspar-quartz gneiss, chlorite, sillimanite, andalusite, muscovite-biotite granite and pegmatite; amphibolite.|
22638|Penny Gneiss|71792|4|Described|p3-p4|Mesoproterozoic|Paleoproterozoic|Etheridge Province. A metamorphic crystallisation age of 1561 Ma is provided.|1639 Ma (Magmatic crystallisation)|Newberry Metamorphic Group||Overlain by the Kimba Gneiss.|Banded muscovite-biotite-sillimanite-plagiolcase-K-feldspar-quartz gneiss interlayered with granite and pegmatite.|
22638|Penny Gneiss|71849|5|Briefly described|p8, p98, p195|Mesoproterozoic|Paleoproterozoic|||Newberry Metamorphic Group.||Is intruded by Lankelly Granite.||
22638|Penny Gneiss|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Newberry Metamorphic Group.|||Banded muscovite-biotite-sillimanite-plagioclase-K-feldspar-quartz gneiss; chlorite common; interlayered with muscovite(-biotite) granite and pegmatite; boudins, pods and dykes of garnet amphibolite and quartz.|
36312|Pepper Diorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite?||||||
36312|Pepper Diorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Almaden Supersuite.|||Very dark grey, medium- to coarse-grained pyroxene?-biotite-hornblende diorite and gabbro?; commonly partly altered and/or recrystallised.|
36636|Pepper Pot Mountain granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 500.  I-Type.||||||
75725|Perch Creek Granodiorite|70740|5|Briefly described|p128|||Outcrop characteristics and distribution briefly discussed. Probably intrudes the Earlscliffe Dacite. |||||Fine to medium-grained, porphyritic biotite-hornblende granodiorite to quartz monzodiorite with numerous mafic inclusions.|
78397|Percol Plains Tonalite|64250|6|Mentioned|p11 fig.3|||Cloncurry Fold Belt, Eastern Fold Belt, Mount Isa Inlier.|1552 +/- 42 Ma.|||||16-OCT-13
78397|Percol Plains Tonalite|65396|6|Mentioned|p7, p82, p84, p157, p175, p241|Calymmian|Calymmian|Cloncurry Fold Belt. Eastern succession. Appears as Percol Planes Tonalite on p157.|1552 +/- 42 Ma|||||
78397|Percol Plains Tonalite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt. [Written as Percol Pains Tonalite].|1552 +/- 42 Ma|||||
80220|Percy Douglas Tonalite|70740|5|Briefly described|p20, p28-p29, p32, p34|Permian|Carboniferous|Previously included in the Percy Douglas Granodiorite. Outcrop characteristics briefly discussed. See also p24, p49, p73, p120, p128.||||Intrudes the Les Jumelles beds, Anakie Metamorphic Group, Mount Wyatt Formation, Bimurra Volcanics and the Ukalunda Formation.|Grey, medium-grained, equigranular to seriate, hornblende-biotite tonalite.|05-OCT-17
80220|Percy Douglas Tonalite|73035|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, medium-grained, equigranular to seriate, hornblende-biotite tonalite.|
40274|Percy Group|23911|6|Mentioned|p88 Fig. 2|||Geological Province: Whitsunday Volcanic Province.||||||
38241|Percy Suite|23422|5|Briefly described|p217 Table 6.11|Early Carboniferous|Early Carboniferous|||||||
38241|Percy Suite|69593|6|Mentioned|p495|Carboniferous|Carboniferous|Identified in basaltic-andesitic rocks within Carboniferous sedimentary/volcanic units in the Charters Towers region; Broken River Province.||||||
28011|Permana Granodiorite|23420|5|Briefly described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Staaten Metamorphics||||||
28011|Permana Granodiorite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Sugrabag Creek Quartzite and Wulpan Monzogranite(?). Dark grey, equigranular hornblende-biotite granodiorite.||||||15-JAN-09
28011|Permana Granodiorite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
69838|Perwillowen Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||30-NOV-05
69838|Perwillowen Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Rhyolite tuff.|
69838|Perwillowen Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
31364|Peters Creek Greenstone|22845|2|Defined|p7-9,39-42,77|||After Sliwa (1994),  Intruded by Tungi Creek Granodiorite, Neurum Tonalite, correlates with Rocksberg Greenstone||||||
31364|Peters Creek Greenstone|22846|6|Mentioned|p47|Carboniferous|Devonian|Intruded by Tungi Creek Granodiorite.||||||
31364|Peters Creek Greenstone|43588|6|Mentioned|p30||Late Devonian|||||||
31364|Peters Creek Greenstone|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
31364|Peters Creek Greenstone|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Rocksberg Greenstone, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
31364|Peters Creek Greenstone|68679|5|Briefly described|p321, p326-327, p330-331|||Sliwa (1994); Donchak et al. (1995). Occurs as a series of polydeformed mafic lenses, NW of Conondale, northern New England Orogen. Detachment zone and lower plate accretionary assemblages.||||Is faulted against Jimna Phyllite. Is intruded by Tungi Creek Granodiorite and Neurum Complex. Enclosed within Booloumba beds. Correlated with Rocksberg Greenstone.|Dark green, massive to strongly foliated, commonly coarse-grained metagabbro and volcaniclastic rocks with subordinate jasper and schist. The greenstones have a chlorite-actinolite-albite assemblage with relict clinopyroxene.|
27878|Petford Granite|23423|5|Briefly described|p306 Table 7.3|||Intrudes Tennyson Volcanic Subgroup and Boonmoo Volcanic Subgroup.||||||
27878|Petford Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 299+/-6 Ma, Rb-Sr. of Ootann Supersuite.||||||
27878|Petford Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite. Age: 299+/-6Ma.||||||
27878|Petford Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 329. I-Type.||||||
27878|Petford Granite|23616|6|Mentioned|Table 3 p48|||||||||
27878|Petford Granite|29605|6|Mentioned|Table 3|||||||||
27878|Petford Granite|39564|4|Described|p7|||||||||
27878|Petford Granite|41235|6|Mentioned|p42|||||||||
27878|Petford Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite).  Pale grey to pink-grey, abundantly porphyritic hornblende-biotite granite. Age: 299+/-6Ma.||||||15-JUN-06
27878|Petford Granite|43259|4|Described|Appendix 1,p39.||Late Carboniferous|Age is 299+/-6 Ma.||||||
27878|Petford Granite|43626|6|Mentioned|p10||Late Carboniferous|||||||
27878|Petford Granite|60425|4|Described|p47 and 49 Tb. 3, p278-9 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).Age: 299+/-6Ma (Rb-Sr). Intrudes Tennyson Volc.Subgp. Also intruded Boonmoo Volcanic Subgp.I-type. Two subunits:(1) highly porph'ic hornblende-biotite granite (2)fine- to med-gr., even-gr., (hornblende-)biotite granite.||||||07-FEB-11
27878|Petford Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The two variants are mapped separately.|305 +/- 6 Ma (Rb-Sr, total rock).|Unit in Ootann Supersuite.|||Pale grey to pinkish grey, highly porphyritic hornblende-biotite monzogranite; minor fine-grained moderately porphyritic variant with scattered mafic inclusions up to ~10 cm across.|
27878|Petford Granite|68576|5|Briefly described|Q_11: p13|||Petford area. Forms hilly country.|305 +/- 6 Ma (Rb-Sr age).||||Pink to grey, porphyritic hornblende-biotite granite.|
29430|Phar Lap Member|23032|5|Briefly described|p28|Devonian|Devonian|Now considered to be at base of Papilio Mudstone, instead of at top of Dosey Limestone and Burges Formation.||||||
29430|Phar Lap Member|23424|5|Briefly described|p336|||Originally placed at the top of the Dosey Limestone, but now considered to be at the base of the Papillio Formation?/mudstone. Of Papillio Mudstone/Wando Vale Subgroup.||||||
29430|Phar Lap Member|42933|3|Fully described|Table 2|||See also p108. Member of both Burges Formation & Dosey Limestone.||||||
29430|Phar Lap Member|50093|4|Described|p329 Fig.2|Givetian|Givetian|Thin interbedded mudstones and arenites, and mior rudites. Interpreted as a mixed carbonate-siliclastic intertidal channel deposit. Of Dosey Limestone. Has also been grouped in Papilio Formation. Of Broken River Group.||||||07-FEB-11
29430|Phar Lap Member|63152|5|Briefly described|p120 Fig. 3|Givetian|Givetian|Of the Papillio Formation (Broken River Group). Basal calcareous clastics with limestone clasts derived from Dosel Limestone. Age: middle Givetian.||||||10-APR-07
29430|Phar Lap Member|69592|5|Briefly described|p264-265|Middle Devonian|Early Devonian|Wade Anticlinorium; Graveyard Creek Subprovince, Broken Creek Province. A distinctive unit in the upper part of the Formation. Tidal channel deposits in a regressive phase.||Burges Formation.|||Distinctive, thin- to medium-bedded, bidirectional cross-laminated calcareous sandstone; fine- to coarse-grained, moderately to well sorted, feldspathic to lithic; locally contains limestone granules and pebbles; conglomerate interbeds in upper part.|
83936|Phillips seam|70330|6|Mentioned|p12, 16|Late Permian|Late Permian|Bowen Basin. Uppermost seam in the Rangal Coal Measures.||Rangal Coal Measures.||Overlies the Leichhardt seam.||
36269|Phoenician Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|of Cooktown Supersuite.||||||
36269|Phoenician Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite.  Porphyritic biotite granite.||||||
36269|Phoenician Granite|60425|5|Briefly described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Mount Poverty Suite (Cooktown Supersuite). S-type. Med.-gr., even-gr. to slightly porphyritic tourmaline-muscovite-biotite granite; tourm.locally common; extensively altered (greisenised) in places (mainly margins)+ assoc'd cassiterite.||||||07-FEB-11
36269|Phoenician Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Poverty Suite.|||S-type granitoids.|
83680|Phoenix Seam|73305|6|Mentioned|p551, p552 Fig.4, p554 Tb.2, p555-556|Late Permian|Late Permian|Bowen Basin. Second-order coal seam within the Fair Hill Formation split from the FH1 seam [Fair Hill Seam], 1.8 to 3.9 m thick. See also p556 Fig.8.||Fair Hill Formation|||Coal seam.|12-FEB-23
23903|Piano Gully Granodiorite|22847|3|Fully described|p 39|||||||||
23903|Piano Gully Granodiorite|23422|6|Mentioned|p209 Table 6.6|||||||||
23903|Piano Gully Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 89. I-Type.||||||
23903|Piano Gully Granodiorite|42633|5|Briefly described|Table 1 P11|||Reserved.||||||
23903|Piano Gully Granodiorite|42750|2|Defined|p35|Middle Ordovician|Early Ordovician|||||||
23903|Piano Gully Granodiorite|43093|4|Described|Appendix 1||Ordovician|Probable Middle Ordivician||||||
23903|Piano Gully Granodiorite|43259|4|Described|Appendix 1,p21.||Ordovician|originally Weir Granite.||||||
23903|Piano Gully Granodiorite|43933|5|Briefly described|Map Legend||Ordovician|||||||
23903|Piano Gully Granodiorite|43934|5|Briefly described|Map Legend||Ordovician|||||||
23903|Piano Gully Granodiorite|62521|5|Briefly described|p10, p26|Middle Ordovician|Late Cambrian|Formerly called Weir Granite (Hartley and others 1989). Of the Lavery Creek Supersuite. Geological Province: Ravenswood Batholith. Foliated grey, medium-grained, slightly porphyritic hornblende-biotite granodiorite.||||||14-JAN-08
74235|Pickhandle Tonalite|68679|5|Briefly described|p362|||Bowen-Mackay region, Northern Connors Subprovince. Pennsylvanian-early Permian. Has well-developed foliation.|297.1 +/- 1.9 Ma (SHRIMP: Cross et al., 2012).|||||
74235|Pickhandle Tonalite|68901|5|Briefly described|p74|Early Permian|Late Carboniferous|Compared with Pine Creek Granite age (297.2 +/- 1.8 Ma SHRIMP U-Pb), and Urannah Batholith rocks.|(297.1+/-1.9 Ma, unpublished data)|||||16-NOV-18
74235|Pickhandle Tonalite|69952|5|Briefly described|p2 Tb.i, p5, p84-88|Asselian|Asselian|Urannah Batholith, SW of Bowen. New England Orogen. SHRIMP U-Pb zircon magmatic crystallisation age; within error of metamorphism ages for the adjacent Key Creek Gneiss and Dead Horse Gneiss, implying granitoid emplacement and metamorphism were part of the same event.|297.1 +/- 2.0 Ma (Cross et al., 2015).||||Includes quartz diorite, tonalite.|30-NOV-15
74235|Pickhandle Tonalite|70673|5|Briefly described|p5, p118|||Part of the Urannah Batholith. Has well-developed foliation.|297.1 +/- 2.0 Ma (Cross et al., 2015).|||||
74235|Pickhandle Tonalite|71592|5|Briefly described|Appendix A.|||New England Orogen.|297+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Quartz diorite.|
74235|Pickhandle Tonalite|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Grey, fine to medium, slightly porphyritic biotite to biotite-hornblende tonalite to quartz monzodiorite, and hornblende-biotite-clinopyroxene quartz diorite; gneissic in places; traces of titanite, allanite and mafic inclusions to 1m.|
74235|Pickhandle Tonalite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Grey, fine to medium, uneven-grained to slightly porphyritic biotite to biotite-hornblende tonalite to quartz monzodiorite, + hornblende-biotite-clinopyroxene quartz diorite; gneissic in places; traces of titanite, allanite + mafic inclusions to 1m.|
36475|Pieter Botte Supersuite|23423|4|Described|p311 Table 7.4||Late Permian|I-type granite. Intrudes Hodgkinson Formation + Obree Point Volcanics. Also see p251. Granites from this unit were previously included in the Yates Supersuite. Also see p251. Chemically similar to Cape Melville Supersuite.||||||
36475|Pieter Botte Supersuite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Bunk Creek Granite.||||||
36475|Pieter Botte Supersuite|60425|3|Fully described|p54 Tb. 4, p94, p272-3 Appdx. 1|Late Permian|Early Permian|Comprises Bunk Ck, Nulbullul + Thornton Granites. Age: 261+/-3Ma (SHRIMP). Intruded Hodgkinson Fm.+Obree Point Volcs. I-type, fine- to med.-gr., slightly-highly porphyritic biotite-hornblende granite, (hornblende-)biotite granite and biotite leucogranite||||||07-FEB-11
36475|Pieter Botte Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Brodies Camp, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36475|Pieter Botte Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.||||Intrudes Normanby Formation.|I-type granitoids.|
36475|Pieter Botte Supersuite|69593|5|Briefly described|p478, p480, p482-483|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~130 km2 forming mountains and ranges in eastern Hodgkinson Province. Age from constituent Nulbullulul Granite).|261 +/- 3 Ma (SHRIMP U-Pb zircon).||Nulbullulul Suite.||I-type. Hornblende-biotite and (hornblende-)biotite granite, biotite leucogranite.|
36475|Pieter Botte Supersuite|73197|6|Mentioned|p476 Fig.7|Middle Triassic|Lopingian||||||Intrusives.|
82721|Pike Creek Dolerite|71628|5|Briefly described|p5: 7; p19: 145-146|||New (previously unpublished) name, after Butler (1974, unpublished). Named after a local watercourse. Located ~5 km W of Pikedale. Forms a long dyke-like series of at least six small bodies. Limited (two analyses) geochemistry briefly described.||Pike Creek Suite.||Intrudes Texas beds. Mostly enclosed by Mount You You Leucogranite (relationship unknown).|Medium-grained dolerite to gabbro with a well-developed interstitial texture.|
22655|Pillar Granodiorite|43087|6|Mentioned|p54|||Informal name of Richards (1981).||||||
22655|Pillar Granodiorite|43259|6|Mentioned|Appendix 1,p47.||Carboniferous|of Hiker Granodiorite.||||||
77817|Pilpah Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin|||||Fine to coarse-grained, medium to thick-bedded sandstone with minor siltstone.|
77817|Pilpah Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Saint-Smith and Bularnu Formations under the symbol, -Pp.||||||
77817|Pilpah Formation|69591|5|Briefly described|p29, p56|Paleoproterozoic|Paleoproterozoic|Mount Oxide Domain, Mount Isa Province. Part of the ?Prize Supersequence. Fluvial/shallow-marine deposits.|||||Fine- to coarse-grained, medium to thick bedded sandstone with minor siltstone.|
77817|Pilpah Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
22657|Pinchgut Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite.||||||
22657|Pinchgut Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
22657|Pinchgut Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 437. I-Type.||||||
22657|Pinchgut Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22657|Pinchgut Granite|43083|5|Briefly described|p255|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
22657|Pinchgut Granite|43087|2|Defined|p61|Late Carboniferous||||||||
22657|Pinchgut Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22657|Pinchgut Granite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
22657|Pinchgut Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Fine-grained leucogranite absd aplitic leucogranite; granophyric in part; commonly altered with sericite and chlorite common; minor U mineralisation, mainly along joints and fractures.||||||07-FEB-11
22657|Pinchgut Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to pale grey, fine-grained (biotite-)leucogranite, aplite leucogranite; granophyric in part; generally altered with chlorite and sericite common.|
26320|Pindari Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26320|Pindari Formation|36925|2|Defined|p180|Early Permian|Early Permian|||||||
26320|Pindari Formation|38204|4|Described|p73|||||||||
26320|Pindari Formation|38310|6|Mentioned|p237|||||||||
26320|Pindari Formation|38917|6|Mentioned|p168|||||||||
26320|Pindari Formation|40091|5|Briefly described|p71|||||||||
26320|Pindari Formation|40093|4|Described|p30|||||||||
26320|Pindari Formation|41246|6|Mentioned|Map legend|Permian||||||||
26320|Pindari Formation|41546|4|Described|p157|||||||||
26320|Pindari Formation|41666|6|Mentioned|Fig.1|||||||||
26320|Pindari Formation|43017|5|Briefly described|Fig.3,p375|||||||||
26320|Pindari Formation|64856|5|Briefly described|p48|||Flood et al. (1981). Overlies Buffel Formation where locally developed.| | ||||29-NOV-17
26320|Pindari Formation|65388|5|Briefly described|p160, 165|Kungurian|Kungurian|Of Back Creek Group, Bowen Basin. Of Flood & others (1981), Briggs (1993). Disconformable over Buffel Formation. Conformably overlain by Oxtrack Formation.  Regarded by Draper (pers. comm., 2000) as possibly part of Oxtrack Formation. Status of this unit not resolved in this study.||||||
26320|Pindari Formation|68679|5|Briefly described|p378|||Flood et al. (1981). Bowen Basin. 100m thick. Marine shelf deposits.|||||Spicule-rich sandstone, siltstone.|
75767|Pine Creek Granite|68679|5|Briefly described|p362|Permian|Pennsylvanian|Kennedy Igneous Association.|297.2 +/- 1.8 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75767|Pine Creek Granite|68901|5|Briefly described|p4, p73-p76, p146|Early Permian|Late Carboniferous|New England Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail. Age compared with Pickhandle Tonalite age (297.1+/-1.9, unpublished data).|297.2 +/- 1.8 Ma (SHRIMP U-Pb)||||Pale-pink, medium-grained, moderately porphyritic biotite monzogranite characterised by phenocrysts of pale pink K-feldspar, plagioclase, glassy quartz and scarce miarolitic cavities.|15-NOV-18
75767|Pine Creek Granite|69593|5|Briefly described|p513|||Burdekin Falls Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|297 +/- 2 Ma.||||I-type.|
75767|Pine Creek Granite|70740|5|Briefly described|p128|||Outcrop characteristics and distribution briefly discussed. |||||Mainly medium-grained, porphyritic biotite and hornblende-biotite monzogranite with rare mafic inclusions.|
75767|Pine Creek Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|297+/-1.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
34633|Pine Mountain Serpentinite|22845|6|Mentioned|p33|Carboniferous|Devonian|Similar to the Mount Mia Serpentinite.||||||
34633|Pine Mountain Serpentinite|68679|5|Briefly described|p329|||Between the Ipswich Basin and South D'Aguilar Subprovince.||||Correlated with Mount Mia Serpentinite.||
25400|Pine Ridge Sandstone Member|31116|6|Mentioned|p20|||||||||
25400|Pine Ridge Sandstone Member|31369|2|Defined|p88|Middle Triassic|Middle Triassic|See also P34.||||||
36650|Pine Tree Creek Granite|23420|4|Described|p 152 table 4.8||Early Devonian|Informal name[?] Intrudes Burton Lagoon Granite. Intruded by Artella Granite.||||||27-FEB-09
36650|Pine Tree Creek Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
32130|Pinedale Granite|23037|4|Described|p82,7|Permian||||||||28-NOV-06
32130|Pinedale Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgpd].  Pink to grey, porphyritic bitotite granite with large K-feldspar phenocrysts.||||||
32130|Pinedale Granite|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Overlies Wingfiled Granite.||||||17-MAY-04
32130|Pinedale Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to grey, porphyritic, biotite granite with large K-feldspar phenocrysts.||||||
32130|Pinedale Granite|60282|6|Mentioned|p22|||||||||
32130|Pinedale Granite|61087|5|Briefly described|Map Legend|Permian|Carboniferous|Pink to grey, porphyritic biotite granite with large K-feldspar phenocrysts.||||||
32130|Pinedale Granite|65388|2|Defined|p271-272, p236, 237, 238, 248, 259, 263|Early Permian|Late Carboniferous|Interpreted as older than Dawson Granite. Intruded by Montour Gabbro, Keen Creek Granite. Relationship to Jonah Vale Granite to N and W is not known. Radiometric response compared with Hildura Quartz Monzodiorite. Tentative age assigned, but could be older. Grey and pink, medium grained biotite granite with pink K-feldspar phenocrysts.||||||
32130|Pinedale Granite|68679|5|Briefly described|p404, p406-408|Permian|Carboniferous|Auburn Subprovince, New England Orogen. Weakly foliated; may indicate older age.||||Intrudes Montour Gabbro. Is intruded by Keen Creek Granite.|I-type. Grey and pink, medium-grained biotite granite with pink alkali feldspar phenocrysts.|
36528|Pink Lily complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 183.||||||
38322|Pinnacle Creek Suite|23291|4|Described|p100 Tb. 3.12|Late Carboniferous|Late Carboniferous|See also Pinnacle Creek Suitte (misspelt). Parent: O'Briens Creek Supersuite. Includes the Fulford Creek granite and Square Rock granite. Geological Province: Georgetown Region.||||||08-JUL-15
36574|Pinnacles Porphyry|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 287.  I-Type.||||||
36574|Pinnacles Porphyry|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Brien's Creek Supersuite||||||
36574|Pinnacles Porphyry|60425|6|Mentioned|p287 Appdx.|||Mentioned as informal name for Neds Gully Granite (of Ravenshoe Suite, O'Briens Creek Supersuite). Not to be confused with Pinnacles Granite of Go Sam Suite (O'Briens Creek Supersuite). Written informally as Pinnacles porphyry.||||||07-FEB-11
80259|Pisces Seam|70861|6|Mentioned|p38,40,42-43|Late Permian|Late Permian|Of Bowen Basin.||Shown as part of Burngrove Formation.||Yarrabee Tuff overlies.||29-AUG-19
80259|Pisces Seam|70940|6|Mentioned|p844|Late Permian|Late Permian|Southern Bowen Basin. Contains the Yarrabee Tuff marker bed.|||||Coal.|06-OCT-17
80259|Pisces Seam|72297|5|Briefly described|p695|Permian|Permian|Bowen Basin.||Rangal Coal Measures.||||
80259|Pisces Seam|73305|6|Mentioned|p554 Tb.2, p559 Fig.11, p560|Late Permian|Late Permian|Bowen Basin. Denison and Taroom Troughs. 1.3 to 7.4 m thick. Correlative with the Vermont Seam. Split by the Yerrabee Tuff into an upper and lower seam. The Pisces Seam only splits into upper and lower parts in the in the Denison and Taroom troughs.||||Correlated with Vermont Seam|Coal seam.|
83674|Pisces Seam, Lower|73305|6|Mentioned|p555 Fig.7, p556 Fig.8, p559, p560|Late Permian|Late Permian|Bowen Basin. Diverges from the Yarrabee Tuff in the northern Taroom Trough by over 15 m. See also p559 Fig.11.||Burngrove Formation||||
35195|Pisgah Igneous Complex|23042|4|Described|p97,8 Fig 2||Late Carboniferous|Overlying unit Lizzie Creek Volcanics.||||||
35195|Pisgah Igneous Complex|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35195|Pisgah Igneous Complex|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink, medium- to coarse-grained leucocratic syenogranite, biotite granite and minor biotite-hronblende granodiorite (also common as zenoliths in the granite); common pegmatite and aplite; rhyolite, andesite and basalt dykes.||||||16-MAR-06
35195|Pisgah Igneous Complex|65388|2|Defined|p379-380, p135, 362, 364, 365, 371, 381|Early Permian|Early Permian|Northern Connors Arch. Southern Urannah Batholith. Yarravale Creek Granite, Uruba Granite and Screaming Creek Gabbro probably younger, based on pluton shape. Separates two outcrops of Gargett Granite. May be intruded by Teemburra Igneous Complex. Probably intrudes Leura Volcanics. May be overlain by Mount Benmore Volcanics. Probable age given. Pink, medium to coarse-grained biotite granite at type locality. Se also p382, 386, 388.||||||
35195|Pisgah Igneous Complex|73037|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Shown at Subgroup rank.|||||Pink, medium to coarse-grained leucocratic syenogranite, biotite granite and minor biotite-hornblende granodiorite (also common as xenoliths in the granite); common pegmatite and aplite; rhyolite, andesite and basalt dykes.|
36141|Platypus Tuff Bed|23444|2|Defined|p183|Late Permian|Late Permian|Of Moranbah Coal Measures.  Geological province: Bowen Basin.||||||25-SEP-06
36141|Platypus Tuff Bed|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of Moranbah Coal Measures (Blackwater Group).  Age: ~259Ma.  Geological Province: Bowen Basin.||||||
36141|Platypus Tuff Bed|65388|4|Described|p199|||Of Moranbah Coal Measures. Formalised by Michaelsen &others (2001). 1-1.5mm thick, forms an important marker traceable for over 300km along strike. It was originally referred to as the "P Tuff". SHRIMP U/Pb age: 258.9+/- 2.7 Ma. Tuffaceous mudstone and contains 10-15% quartz crystal fragments that are up to 1mm and euhedral bronze biotite.||||||
36141|Platypus Tuff Bed|68679|5|Briefly described|p376, p382|||Formally defined as the Platypus Tuff Bed by Michaelson et al. (2001). Previously the P-tuff of Koppe (1978), used for correlation purposes. Similar age as Wallabella Coal Member (Tinowon Formation). Appears as Platypus Tuff bed on p382.|258.9 +/- 2.7 Ma (Michaelson et al., 2001).|||||
36141|Platypus Tuff Bed|75060|6|Mentioned|p46, 57|||Bowen Basin. A regional marker horizon.|258.9 +/- 2.7 Ma (Michaelsen et al., 2001).|||||
30709|Playboy Granite|24197|5|Briefly described|p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30709|Playboy Granite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||
30709|Playboy Granite|50332|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760-1720Ma. Intruded into the Kalkadoon-Ewen Province and Eastern Fod Belt Province. Geological Province: Kalkadoon-Ewen Province and Eastern Fod Belt Province.||||||07-FEB-11
30709|Playboy Granite|50536|5|Briefly described|p1.4, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite. Age: 1742 +/- 13Ma (U-Pb).||||||07-NOV-08
30709|Playboy Granite|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||Mary Kathleen Domain, Mount Isa Inlier.|1742 +/- 13 Ma.|Wonga Suite.||Intrudes Corella Formation.||
30709|Playboy Granite|69056|5|Briefly described|Time-Space plot sheet|Statherian|Statherian||1742 +/- 13 Ma; 1740 +/- 3 Ma.|||Intrudes Corella Formation.||
30709|Playboy Granite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Kalkadoon-Leichhardt and Mary Kathleen Domains.|1742+/-13 Ma crystallisation age||||Felsic intrusion.|
30709|Playboy Granite|73553|4|Described|p18, p35-36, p65, p73-p75,|Statherian|Statherian|Mary Kathleen Domain. Wonga Igneous Subprovince. Small, elongate roughly north-south oriented body ~10 km long and ~ 3 km wide. Formerly mapped as undivided Wonga Granite (GSQ, 2018). Distribution based on Bastrakova et al., (2001) and detailed geological boundaries (GSQ, 2018). Truncated by the Wonga Fault in the north. Generally white to slightly yellowish tones on radiometric images. Low magnetic response with irregular bodies of slightly elevated magnetic respose. See also p80-81, p86-88, p118, p246-247, p249.|1742+/-13 Ma U-Pb zircon (Pearson et al., 1992)|||Interpreted to intrude Argylla Formation|Foliated, coarse-grained to pegmatitic biotite syenogranite; mingled coarse- and fine-grained foliated biotite syenogranite with local mafic domains.|03-FEB-23
70106|Plevna beds|61917|5|Briefly described|Map legend|Tertiary|Tertiary|Carbonaceous mudstone, oil shale, tuffaceous siltstone and minor sandstone.||||||
70106|Plevna beds|69599|5|Briefly described|p592|Oligocene|Oligocene|Exposed in the deeply incised valley of Hazlewood Creek on the Eungella Tableland. Up to 95.7m thick. Previously regarded as early Miocene from palynomorphs (Hekel, 1972); revised age from dating of overlying basalt at 27.7 +/- 0.7 Ma by Sutherland et al. (1977).|||||Interbedded, low-grade oil shale, tuffaceous shale, mudstone, carbonaceous shale and minor sandstone.|
24459|Plum Mountain Gneiss|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24459|Plum Mountain Gneiss|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24459|Plum Mountain Gneiss|37862|4|Described|p581|||||||||
24459|Plum Mountain Gneiss|38234|4|Described|p103|||||||||
24459|Plum Mountain Gneiss|38310|6|Mentioned|p237|||||||||
24459|Plum Mountain Gneiss|38350|4|Described|p7|||||||||
24459|Plum Mountain Gneiss|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24459|Plum Mountain Gneiss|38900|6|Mentioned|p62|||||||||
24459|Plum Mountain Gneiss|39445|5|Briefly described|Table 2|||||||||
24459|Plum Mountain Gneiss|40840|6|Mentioned|Map legend|||||||||
24459|Plum Mountain Gneiss|41381|6|Mentioned|p325|||||||||
24459|Plum Mountain Gneiss|41978|6|Mentioned|p495|||||||||
24459|Plum Mountain Gneiss|41979|6|Mentioned|Fig.2 P512|||||||||
24459|Plum Mountain Gneiss|42565|5|Briefly described|Table 1 P6|||||||||
24459|Plum Mountain Gneiss|43619|6|Mentioned|p43||Precambrian|||||||
24459|Plum Mountain Gneiss|45161|4|Described|p16|||||||||
24459|Plum Mountain Gneiss|45166|4|Described|p10|||||||||
24459|Plum Mountain Gneiss|49009|2|Defined|p35|Proterozoic|Proterozoic|See also p36.||||||02-APR-07
24459|Plum Mountain Gneiss|49041|5|Briefly described|Table 2|||||||||
24459|Plum Mountain Gneiss|50100|6|Mentioned|p11, p14|Proterozoic|Proterozoic|Intruded by granites of the Wonga and Kalkadoon Batholiths.||||||
24459|Plum Mountain Gneiss|50536|5|Briefly described|p6.3|||Geological Province: Mount Isa Inlier. Intruded by Burstall Suite.||||||02-APR-07
24459|Plum Mountain Gneiss|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Mainly felsic gneiss, augen gneiss, and foliated granite.||||||
24459|Plum Mountain Gneiss|60513|6|Mentioned|p281, 283, p281 fig 2, p289, p287, 288|||||||||
24459|Plum Mountain Gneiss|61933|5|Briefly described|p169 Fig.1|||||||||
24459|Plum Mountain Gneiss|63593|6|Mentioned|p289.|||Part of basement of Mount Isa Inlier.||||||
24459|Plum Mountain Gneiss|63866|6|Mentioned|p59|||Mary Kathleen Belt.||||||
24459|Plum Mountain Gneiss|64248|6|Mentioned|p32, p38 Fig.5, p39, p43 Fig.11, p45|||Oldest basement rocks exposed in this study area. Deformed and metamorphosed in Barramundi Orogeny c.1900-1870 Ma.||||Is overlain by Leichhardt Volcanics. Is intruded by Kalkadoon Granite.||11-DEC-17
24459|Plum Mountain Gneiss|64250|6|Mentioned|Figs.1,3, 4; p8, p11, p19|||A basement unit of Kalkadoon-Leichhardt Belt, Mt Isa Inlier. Discussed with Kurbayia Migmatite which has date on metamorphism of 1890 +/- 8 Ma. Correlation implied.||||||14-MAR-18
24459|Plum Mountain Gneiss|64254|5|Briefly described|p160 Fig. 1, p165|Paleoproterozoic|Archaean|Age: 2380-2820Ma (Nd model). Geological Province: Kalkadoon - Leichhardt Belt.||||||
24459|Plum Mountain Gneiss|65396|5|Briefly described|p82, p171-172, p175, p186, p219, p222|||See also p241, p437-438. Kalkadoon-Leichhardt Belt. Also spelled Plumb Mountain Gneiss. Basement to the Eastern Succession, Mount Isa Inlier.||||||07-OCT-22
24459|Plum Mountain Gneiss|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p29|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Kalkadoon Igneous Event. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny.||Kalkadoon Supersuite|||Quartzofeldspathic gneiss, augen gneiss, weakly foliated to gneissic even-grained and porphyritic granite; minor calc-silicate rocks, meta-arenite, mica schist, amphibolite; aplite and pegmatite veins.|
24459|Plum Mountain Gneiss|68146|5|Briefly described|p1, p6, p50-56, p193, p211|||Part of the crystalline basement of the Kalkadoon-Leichhardt Domain. Crops out as low boulders on an alluvial plain. Whole-rock Sm-Nd isotopic data tabulated.|1862 +/- 3 Ma protolith emplacement.||||Gneissic granite: very strongly deformed, cream coloured, megacrystic biotite augen gneiss.|
24459|Plum Mountain Gneiss|69591|5|Briefly described|p29-30, p60|||Kalkadoon Batholith. One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma).|1862 +/- 3 Ma (Carson et al., 2011).||||Quartzofeldspathic gneiss, augen gneiss, weakly foliated to gneissic even-grained and porphyritic granite; minor calc-silicate rocks, meta-arenite, mica schist, amphibolite; aplite and pegmatite veins.|
24459|Plum Mountain Gneiss|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1862+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
24459|Plum Mountain Gneiss|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||||Shown as older than the Argylla Formation. Shown as as age equivalent to Kalkadoon Granite, Woonigan Granite, Mayfield Gneiss.|Quartzofeld spathic gneiss, augen gneiss, weakly foliated to gneissic even-grained and porphyritic granite; minor calc-silicate rocks, meta-arenite, mica schist, amphibolite; aplite and pegmatite veins.|
24459|Plum Mountain Gneiss|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain.||||Shown as older than the Argylla Formation. Shown as age equivalent to Kalkadoon Granite, Woonigan Granite, Mayfield Gneiss.|Quartzofeldspathic gneiss, augen gneiss, weakly foliated to gneissic even-grained and porphyritic granite; minor calc-silicate rocks, meta-arenite, mica schist, amphibolite; aplite and pegmatite veins.|
24459|Plum Mountain Gneiss|72919|6|Mentioned|p7|Orosirian|Orosirian|Mount Isa Province. An age of 1862 +/- 3 Ma was reported by Carson et al. (2011).|1862 +/- 3 Ma|||||
24459|Plum Mountain Gneiss|73137|6|Mentioned|p1|||Intruded by igneous rocks of similar age ( (1863+/- 6 Ma) that are [tentatively] assigned to the Birds Well Granite. Similar in age to One Tree Granite.||||||07-OCT-22
24459|Plum Mountain Gneiss|73413|6|Mentioned|p3, p5-6, p21, p23, App.1|Orosirian|Orosirian|[Also written as Plum Mountain gneiss]. Mount Isa Inlier, Kalkadoon-Leichhardt Belt. A U-Pb zircon age of 1862 +/- 3 Ma from 20 km northwest of Tick Hill was reported by Carson et al. (2011).|1862 +/- 3 Ma U-Pb zircon|||Intruded by Saint Mungo Granite.||
24459|Plum Mountain Gneiss|73525|6|Mentioned|p4, p19 Fig.13|||Kalkadoon-Leichhardt Domain.|||||Metamorphics.|
24459|Plum Mountain Gneiss|73553|4|Described|p8 Fig.1.2.3, p14, p47, p49-50,|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain, southern. Syn- or pre- Barramundi Orogeny. Previously mapped as Kalkadoon Granite, tentatively correlated with Wonga Granite (Carter and Opik, 1963). Crops out in NNW-trending belt. A western belt is now assigned to the Blaze Creek Gneiss. Included in the Kalkadoon Supersuite in the GSQ report of 2011. Distinguished by red tones on radiometric images. Very low response on aeromagnetic images indistinguishable from adjacent units. Interpreted as metamorphosed granitic intrusions, range of lithologies reported and may include metamorphosed felsic volcanics; metasedimentary rocks are currently included in the Corella Formation. Interpreted to be intruded by One Tree Hill Granite, Saint Mungo Granite, and Birds Well Granite? as well as mafic dykes (Blake et al., 1982a). See also p53, p250-254, p257-258.|~1865 Ma U-Pb zircon, 1864+/-3 Ma LA-ICP-MS|Kalkadoon Supersuite||Intruded by Saint Mungo Granite|Fine- to coarse-grained megacrystic gneiss and quartzofeldspathic gneiss, generally appears massive and is in places crenulated.|03-FEB-23
23910|Pocket Dam Granite|22847|3|Fully described|p 43|Early Ordovician||||||||
23910|Pocket Dam Granite|23422|5|Briefly described|p172, p209 Table 6.6|Middle Ordovician|Early Ordovician|Of Hogsflesh Supersuite. Age: 480 +/- 5Ma (U-Pb zircon).||||||
23910|Pocket Dam Granite|23430|5|Briefly described|p482|||I-Type granite. Ravenswood Batholith Province.||||||
23910|Pocket Dam Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 102. I-Type.||||||
23910|Pocket Dam Granite|42245|2|Defined|p34|Ordovician||||||||
23910|Pocket Dam Granite|43093|4|Described|Appendix 1|||Rb-Sr age of 480+/-5Ma.||||||
23910|Pocket Dam Granite|43259|4|Described|Appendix 1,p22.||Ordovician|Rb-Sr minimum age of 480+/-5 Ma.||||||
23910|Pocket Dam Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
23910|Pocket Dam Granite|68731|6|Mentioned|p150|Ordovician|Ordovician||||||I-type granite.|
22666|Poddskles Microgranite|22847|3|Fully described|p 41|||||||||
22666|Poddskles Microgranite|23422|6|Mentioned|p209 Table 6.6|||||||||
22666|Poddskles Microgranite|23504|5|Briefly described|Map Legend||Ordovician|||||||
22666|Poddskles Microgranite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 493.  I-Type.||||||
22666|Poddskles Microgranite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Early to Middle Ordovician||||||
22666|Poddskles Microgranite|43936|5|Briefly described|Map Legend||Ordovician|||||||
22670|Poison Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive 138. I-Type.||||||
22670|Poison Creek Granite|23617|3|Fully described|p23-24||Carboniferous|Also see Table 2 p18. Intrudes Kangaroo Hills Formation and is cut by Ryeburn Quartz Diorite. Table 3 p52. K-Ar 289 +/- 9 Ma. Of Oweenee Supersuite Kennedy Province.||||||
22670|Poison Creek Granite|23618|5|Briefly described|map legend||Carboniferous|||||||
22670|Poison Creek Granite|43259|4|Described|Appendix 1,p25.||Carboniferous|||||||
22670|Poison Creek Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
23914|Poley Cow Formation|13996|6|Mentioned|p131, p143-144|||Broken River area. Contains numerous graptolite taxa, of which 75% have European affinities. Biogeographic implications discussed. Hosts Llandovery-aged trilobites. Biogeographic affinities.||||||
23914|Poley Cow Formation|23032|4|Described|p21,24|Llandovery|Llandovery|||||||
23914|Poley Cow Formation|23424|4|Described|Table 8.1 p334.||Llandovery|Age: Early Silurian (late Llandovery), conodonts, graptolites and trilobites. Overlies (unconformably) the Judea Fm and Netherwood tonalite. Of Graveyard Creek Group, Graveyard Ck Subprovince. Overlies Jack Fm (c). Max. thickness 680 m.||||||
23914|Poley Cow Formation|23430|5|Briefly described|p476|||Underlying Unit Jack Formation. Broken River Province. Maximum thickness 1 km.||||||
23914|Poley Cow Formation|23431|5|Briefly described|p541|||||||||
23914|Poley Cow Formation|23737|5|Briefly described|p87|Llandovery|Llandovery|||||||
23914|Poley Cow Formation|24029|5|Briefly described|p111, p113 Fig.1, p114|Telychian|Telychian|Of Graveyard Creek Group. See also p115 Fig.3. Mapped seperately by these authors, but considered to be one and the same with Quinton Formation by others such as Simpson (1999) supported by Sloan et al (1995).||||||
23914|Poley Cow Formation|24577|6|Mentioned|p754 Fig. 2|Silurian|Silurian|Also known as the Quinton Formation.||||||
23914|Poley Cow Formation|41260|3|Fully described|p42|||||||||
23914|Poley Cow Formation|41679|6|Mentioned|Fig.2|||||||||
23914|Poley Cow Formation|41719|2|Defined|p217|Early Silurian||||||||
23914|Poley Cow Formation|41739|6|Mentioned|Fig.2|||||||||
23914|Poley Cow Formation|41740|6|Mentioned|p222|||||||||
23914|Poley Cow Formation|42054|6|Mentioned|p273|||||||||
23914|Poley Cow Formation|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
23914|Poley Cow Formation|42709|6|Mentioned|map legend|||||||||
23914|Poley Cow Formation|42933|2|Defined|p62|Early Silurian||of Graveyard Creek Formation||||||
23914|Poley Cow Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Graveyard Creek Group.||||||
23914|Poley Cow Formation|63083|6|Mentioned|p218|Telychian|Telychian|In Broken River region of Qld. Contains Llandovery trilobite fauna.||||||07-FEB-11
23914|Poley Cow Formation|67848|5|Briefly described|p14.|Early Silurian|Early Silurian|Broken River Province. Has late Llandovery fossils.||||Conformably overlies Crooked Creek Conglomerate.||
23914|Poley Cow Formation|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Graveyard Creek Group.|||Mudstone, lithofeldspathic sandstone and polymictic conglomerate; polymictic conglomerate and lithofeldspathic sandstone are separately mapped as an un-named unit.|
23914|Poley Cow Formation|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Graveyard Creek Group.|||Mudstone, lithofeldspathic sandstone and polymictic conglomerate; polymictic conglomerate and lithofeldspathic sandstone are separately mapped as an un-named unit.|
23914|Poley Cow Formation|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince. The 2 facies are mapped separately.||Of the Graveyard Creek Group. ||Conformably overlain by the Jack Formation.|Mudstone, lithofeldspathic sandstone and polymictic conglomerate; polymictic conglomerate and lithofeldspathic sandstone.|
23914|Poley Cow Formation|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Graveyard Creek Subprovince. The 2 facies are mapped separately.||Of the Graveyard Creek Group. ||Conformably overlain by the Jack Formation.|Mudstone, lithofeldspathic sandstone and polymictic conglomerate; polymictic conglomerate and lithofeldspathic sandstone.|
23914|Poley Cow Formation|69030|5|Briefly described|p6|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province).||Graveyard Creek Group||||
23914|Poley Cow Formation|69592|5|Briefly described|p259-262, p267|Silurian|Silurian|Southern Graveyard Creek Subprovince, Broken River Province. 100-700m thick. A variety of Telychian fossil types mentioned.||Graveyard Creek Group.||Overlies Crooked Creek Conglomerate conformably and Judea Formation unconformably. Is overlain conformably by Jack Formation. Lateral equivalent to Quinton Formation.|Mainly medium- to thick-bedded, poorly to moderately sorted, fine- to coarse-grained sandstone, commonly with siltstone interbeds, pebble to cobble conglomerate (sourced from the Judea Formation), and pebbly sandstone.|
23915|Policeman Creek Granodiorite|22847|3|Fully described|p 56|Early Devonian|Late Silurian|||||||
23915|Policeman Creek Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 459. I-Type.||||||
23915|Policeman Creek Granodiorite|42633|5|Briefly described|Table 1 P9|||Reserved.||||||
23915|Policeman Creek Granodiorite|42750|2|Defined|p44|Early Devonian|Late Silurian|||||||
23915|Policeman Creek Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23915|Policeman Creek Granodiorite|43259|4|Described|Appendix 1,p49.|Early Devonian|Late Silurian|||||||
23915|Policeman Creek Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23915|Policeman Creek Granodiorite|62521|5|Briefly described|p18, p21, p55|Early Devonian|Late Silurian|Of Brittania Supersuite. Geological Province: Ravenswood Batholith. Comprises two phases: a northern granite to granodiorite and southern granite.||||||14-JAN-08
41259|Pollard Granodiorite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Porphyritic hornblende-biotite granodiorite.||||||
41259|Pollard Granodiorite|65388|2|Defined|p329-330, 302, 13, 301, 305, 306, 321|Early Triassic|Late Permian| Of Wingfield Suite. Intrudes Yerilla Metamorphics, Nogo beds. Appears to intrude Cheltenham Creek Granite. Probably younger than Coonambula Granodiorite. Rocks previously included in the northern half of the Cheltenham Creek Adamellite. Outcrop poor. Mostly cream to grey, medium to coarse-grained, porphyritic, titanite-bearing, hornblende-biotite granodiorite to monzogranite. See also p338, 339-340.||||||08-SEP-14
41259|Pollard Granodiorite|68679|5|Briefly described|p416, p418-420|||Southern part of the Rawbelle Batholith. ~100 km2; roughly equant pluton much concealed by younger cover. Geochemistry plot.||Wingfield Suite.||Intrudes Cheltenham Creek Granite, Nogo beds, Yerilla Metamorphics.|Porphyritic hornblende-biotite granodiorite. Outcrop poor, weathered and decomposed.|
28027|Pombete Gneiss|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince. May correlate with Chelmsford Gneiss. Intruded by the Arkara Gneiss.||||||
28027|Pombete Gneiss|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
28027|Pombete Gneiss|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
28027|Pombete Gneiss|43596|4|Described|p12-13, p21 Tb. 1||Proterozoic|Of Yambo Metamorphic Group. Comprises grey, fine- to medium-grained sillimanite mica gneisswhich grades locally into garnet-mica schist; garnet porphyroblasts present.||||||27-JAN-09
28027|Pombete Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|Yambo Metamorphic Group||||||24-JAN-05
28027|Pombete Gneiss|50537|6|Mentioned|p6.2|||||||||
28027|Pombete Gneiss|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier.||Yambo Metamorphic Group.||Faulted against Saraga Schist. Is intruded by Arkara Gneiss. May correlate with Chelmsford Gneiss.|Sillimanite(+/- garnet, +/- feldspar) mica gneiss grading into garnet-mica schist; quartzite, amphibolite.|
40132|Pomegranate Tonalite|24615|5|Briefly described|CD|Devonian|Devonian|[Dgpo].  Hornblende-biotite tonalite.||||||
40132|Pomegranate Tonalite|50208|5|Briefly described|Map Legend|Devonian|Devonian|||||||
40132|Pomegranate Tonalite|63600|5|Briefly described|p917|Late Devonian|Middle Devonian|Intrudes the Capella Creek Group. Age: 369.0+/-4.2Ma.||||||07-FEB-11
40132|Pomegranate Tonalite|68008|2|Defined|p71, p315, p317, p319-320,p483,p527,p429|Late Devonian|Late Devonian|New unit. Named after Pomegranate Creek. Small outcrop, 1.5km S of Pomegranate homestead. The type area is a hill at GR249000 73554000 on the Bajool 100k sheet. Forms low hills. Geochemistry compared with Mount Morgan Trondhjemite. Also two K-Ar ages of c.416 Ma by Webb (2012).|369.0 +/- 4.2 Ma (U-Pb zircon).|||Intrudes Balaclava, Mount Hoopbound, Raspberry Creek Formations.|Medium-grained, equigranular tonalite. Massive and apparently undeformed.|
40132|Pomegranate Tonalite|68553|6|Mentioned|Map legend; schematic diagram.|Late Devonian|Middle Devonian|Calliope Province. This unit, as well as the Mount Morgan Trondhjemite and unnamed Middle-Late Devonian plutonic units, are all mapped under the same symbol, Dgm.||||||
40132|Pomegranate Tonalite|68679|5|Briefly described|p312, p399, p401-403|Late Devonian|Middle Devonian|Northern New England Orogen. Small outcrop area near Pomegranate homestead. Geochemically similar to Mount Morgan Trondhjemite to the NW. Low radiometric and magnetic response.|369.0 +/- 4.2 Ma (SHRIMP U-Pb: Fanning, 2012).||||Hornblende-biotite tonalite.|
40132|Pomegranate Tonalite|71592|5|Briefly described|Appendix A.|||New England Orogen.|369+/-4.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
40132|Pomegranate Tonalite|73179|6|Mentioned|p1152|Famennian|Frasnian|New England Orogen, northern. Geochron from Murray et al. (2012).|369.0 +/- 4.2 Ma|||||
30137|Ponto Basalt Member|23422|5|Briefly described|p205 Table 6.3|Early Carboniferous|Early Carboniferous|Of Tareela Volcanics.||||||
30137|Ponto Basalt Member|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group? or Tareela Volcanics. Unsure.||||||
30137|Ponto Basalt Member|24613|3|Fully described|p103-104|Early Carboniferous|Early Carboniferous|Of Tareela Volcanics. Geol.prov: Burdekin Basin. Slightly to moderately porphyritic basalt to andesite, andesitic breccia, amygdaloidal basalt and basaltic andesite, andesitic lapilli tuffs and aphyric basalt to andesite.||||||07-FEB-11
30137|Ponto Basalt Member|43095|2|Defined|p23|Early Carboniferous||Of the Tareela Volcanics, Glenrock Group.||||||21-APR-08
30137|Ponto Basalt Member|43259|6|Mentioned|Appendix 1,p6.||Early Carboniferous|||||||
30137|Ponto Basalt Member|43589|2|Defined|p18|Early Carboniferous|Early Carboniferous|Of the Tareela Volcanics.||||||23-APR-08
30137|Ponto Basalt Member|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.||Of the Tareela Volcanics.||Conformably overlain by the Eridge Volcanic Member.|Dark grey, aphyric to moderately porphyritic basalt and andesite; minor amygdaloidal basalt and andesitic breccia.|
30137|Ponto Basalt Member|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.||Of the Tareela Volcanics.||Conformably overlain by the Eridge Volcanic Member.|Dark grey, aphyric to moderately porphyritic basalt and andesite; minor amygdaloidal basalt and andesitic breccia.|
36169|Poona Creek Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of Almaden Supersuite. after Clarke 1995.||||||02-JUN-09
36169|Poona Creek Granodiorite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Kalunga Suite(Almaden Sup'ste).Age: Late Carb?Fine-/coarse-gr (mainly med.-gr.)hornblende-biotite granodiorite;minor microgranite; delineated as discrete unit by Clarke (1990, 1995); incl. in Saint Patrick Hill granite by Donchak and Bultitude (1998).||||||07-FEB-11
77834|Porcupine Creek Rhyolite|68478|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Brown, grey to purple, generally crystal-rich rhyolitic ignimbrite|
77834|Porcupine Creek Rhyolite|68479|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Brown, grey to purple, generally crystal-rich rhyolitic ignimbrite|
77834|Porcupine Creek Rhyolite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
83550|Porcupine Gorge Formation|73472|2|Defined|p113, p116-122, p124-131, App.1, App.2|Norian|Ladinian|Galilee Basin / Eromanga Basin. Defined herein. Maximum thickness of 18.4 m in the type section at Porcupine Gorge. Named after the type section location. Also known from GSQ Hughenden 6 stratigraphic drill core. Fluvial-floodplain depositional setting. Detrital zircon maximum depositional ages of ca 229.4 +/- 3.6 Ma, 238.7 +/- 3 Ma were reported from near the base of the unit. The basal unconformity marks a significant depositional hiatus of up to 20 million years. Basal pebble conglomerate erosionally incises the Betts Creek beds. Fines upwards. Capped by highly distinctive ca 6.7m of red-orange-coloured sandy siltstone with slickensides and minor mottling interpreted as a well-developed paleosol. Composed of strata previously thought by some to represent the Clematis and/or Rewan groups. Also recognised in GSQ Hughenden 6 core. [See article for palynology and supplementary materials for unit definition].|ca 229.4 +/- 3.6 Ma, 238.7 +/- 3 Ma|||Disconformably underlain by Betts Creek beds. Overlain by Warang Sandstone [paraconformity].|Basal pebble conglomerate, buff-coloured, fine- to medium-grained trough cross-bedded sandstone, carbonaceous mudstone interbedded with sandstone, red-orange-coloured sandy siltstone.|
37277|Port Douglas serpentinite|24003|6|Mentioned|p256 Fig.1|||Informal name||||||
36648|Portland Roads Granite|23420|5|Briefly described|p 147 table 4.6|Permian|Late Carboniferous| In the Weymouth Supersuite.||||||03-JUL-09
36648|Portland Roads Granite|69593|5|Briefly described|p477 Tb.6.2|||Northern Coen region (Jardine Subprovince, Kennedy Igneous Association). |c.285 Ma.|Weymouth Supersuite.||||
28019|Potallah Formation|23420|5|Briefly described|p 142 table 4.4|||In the Edward River Metamorphic Group. Thickness >400m.||||||
28019|Potallah Formation|43596|4|Described|p16, p20 Tb. 1||Proterozoic|Lowest exposed unit of Edward River Metamorphic Group. Conformably overlain by Olkolo Formation. Max. thickness: ~400m. Dominant rock type is fine-grained, grey metasiltstone and quartzite.  Further lithological details included (p20 Tb. 1).||||||27-JAN-09
28019|Potallah Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Edward River Metamorphic Group||||||24-JAN-05
28019|Potallah Formation|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. >400m thick; base not exposed.||Edward River Metamorphic Group.|||Quartzite, slate, chlorite-tremolite metabasalt.|
74676|Pothole Creek Gneiss|63866|5|Briefly described|p59|||Mary Kathleen Belt.|c. 1995 +/- 20 Ma (Crystallisation age)|||||
74676|Pothole Creek Gneiss|64567|5|Briefly described|p1096, 1097|Paleoproterozoic|Paleoproterozoic|Crystallization age 1995 +/-20Ma. Augen gneiss. Intrudes Black Angel Gniess Complex.||||||
74676|Pothole Creek Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p11|Orosirian|Orosirian|Also referred to as Pothole Creek Orthogneiss (in text). Of the Mt Isa region of the North Australian Craton.|2000 - 1970 Ma.|||||11-APR-12
74676|Pothole Creek Gneiss|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Orosirian|Orosirian|Kalkadoon-Leichhardt Domain.|1837+/-10 Ma crystallisation of intrusion age||||Metamorphics.|
26110|Powlathanga Tonalite|22847|3|Fully described|p 55|Early Devonian|Late Silurian|||||||
26110|Powlathanga Tonalite|23505|5|Briefly described|Map legend|Devonian|Silurian|of Amarra Supersuite.||||||
26110|Powlathanga Tonalite|42633|5|Briefly described|Table 1 P8|||Reserved as Powlathanga Granite.||||||
26110|Powlathanga Tonalite|42750|2|Defined|p42|Early Devonian|Late Silurian|||||||
26110|Powlathanga Tonalite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
26110|Powlathanga Tonalite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26110|Powlathanga Tonalite|69592|6|Mentioned|p294|||Ravenswood Batholith. Well-defined gravity lows suggest deep-seated, steep-sided plutons.||||||
22693|Pratt Volcanics|23291|4|Described|p37, p92 Tb. 3.11p|Early Permian|Late Carboniferous|Originally included in the "Featherbed Volcanics". Geological Province: Georgetown Region.||||||08-JUL-15
22693|Pratt Volcanics|23422|5|Briefly described|Plate 7.3|Late Carboniferous|Late Carboniferous|||||||
22693|Pratt Volcanics|23423|4|Described|p309 Table 7.3||Late Carboniferous|Previously included as part of Nychum Volcanics. Also see p335. Underlain by Chillagoe Formation and Quadroy Conglomerate (unconformable). Kennedy Igneous Province.||||||01-JUN-09
22693|Pratt Volcanics|23496|5|Briefly described|Table 3, p47|Late Carboniferous|Late Carboniferous|of Bultitude and Domagala (1988). Previously mapped as part of the Nychum Volcanics.||||||
22693|Pratt Volcanics|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||||||
22693|Pratt Volcanics|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Volcanic No. V134. I-Type.||||||
22693|Pratt Volcanics|23616|5|Briefly described|Table 3 p56||Late Carboniferous|Unconformable on or faulted against Chillagoe Fm and Quadroy Conglomerate; cut by rhyolite dykes. Dargalong Province. Max thickness: <~250 m.||||||30-AUG-04
22693|Pratt Volcanics|23713|4|Described|p8 Table 1||Late Carboniferous|Previously included as part of the Nychum Volcanics. Intruded by Almac Granodiorite.||||||
22693|Pratt Volcanics|24485|3|Fully described|p40, p44 Tb.7|Late Carboniferous|Late Carboniferous|Unconformably underlain by Dargalong Metamorphics and Nundah Granodiorite. Intruded by the Almac Granodiorite. Max Thickness: <~250m. Geological Province: Hodgkinson Province||||||01-JUN-09
22693|Pratt Volcanics|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Geological Province: Kennedy Province.||||||
22693|Pratt Volcanics|43060|5|Briefly described|p73|||||||||
22693|Pratt Volcanics|43083|4|Described|p74|||Probable Late Carboniferous age||||||
22693|Pratt Volcanics|43254|5|Briefly described|map legend||Late Carboniferous|||||||
22693|Pratt Volcanics|43259|4|Described|Appendix 1,p14.||Late Carboniferous|||||||
22693|Pratt Volcanics|43285|5|Briefly described|Map Legend||Late Carboniferous|||||||
22693|Pratt Volcanics|43287|5|Briefly described|Map Legend||Late Carboniferous|||||||
22693|Pratt Volcanics|43625|4|Described|p34|Late Carboniferous||||||||
22693|Pratt Volcanics|43626|4|Described|p92||Late Carboniferous|||||||
22693|Pratt Volcanics|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22693|Pratt Volcanics|60425|4|Described|p40, p50 Tb. 3|Late Carboniferous|Late Carboniferous|Unconformable on Dargalong Metamorphics + Nundah Granodiorite; cut by Almac Granodiorite.Thickness: <~250m. Rhyodacitic to rhyolitic ignimbrite (I-Type) in Cairns area; west of Palmerville Fault contains dacitic to rhyolitic lava flows(A-type)||||||07-FEB-11
22693|Pratt Volcanics|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Georgetown Inlier.||||||
22693|Pratt Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
22693|Pratt Volcanics|69030|6|Mentioned|p6|Permian|Carboniferous|Chillagoe Subprovince, Hodgkinson Province.||||||
22693|Pratt Volcanics|69593|6|Mentioned|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
80636|Precipice Sandstone, Lower|71805|4|Described|p83, p84, p86-p89, p77 fig.3||Sinemurian|Surat Basin. See Precipice Sandstone. Cored in Woleebee Creek GW4. Wireline logs exist for the core and for this unit. Highly varied and greater thickness (<5-115m) than the Upper Precipice Sandstone. Outcrops in the Carnarvon Gorge section of the Carnarvon National Park. An informal lacustrine shale unit seperates this unit and the Upper Precipice Sandstone.||||Overlain by the Precipice Sandstone, Upper.|Fine-grained heterolithic and coarse-grained sandstone.|16-MAY-19
80637|Precipice Sandstone, Upper|71805|4|Described|p80-p82, p84, p86-p89, p77 Fig.3|Toarcian||Surat Basin. See Precipice Sandstone. Cored in Woleebee Creek GW4. Includes fossilised worm burrows including Teichichnid forms which suggest a Triassic age. Wireline logs exist for the core and for this unit. Thickness varies fgrom 10-75m. Part of this unit is interpreted as tidal on the basis of sedimentary structures.||||Overlies the Precipice Sandstone, Lower.|Thinly-bedded sandstone and siltstone in which ripple marks, worm trails and leaf impressions are common.|16-MAY-19
27682|Prestwood Microgranite|23291|4|Described|p48, p98 Tb. 3.11|Late Carboniferous|Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
27682|Prestwood Microgranite|23430|6|Mentioned|p499|||||||||
27682|Prestwood Microgranite|23493|5|Briefly described|p9, p17 Tb. 1|Late Paleozoic|Late Paleozoic|Intrudes Forsayth Granite.||||||07-NOV-08
27682|Prestwood Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 14. I-Type.||||||
27682|Prestwood Microgranite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
27682|Prestwood Microgranite|31832|6|Mentioned|Table 6|||||||||
27682|Prestwood Microgranite|32527|6|Mentioned|p403|||||||||
27682|Prestwood Microgranite|32528|5|Briefly described|Table 1|||||||||
27682|Prestwood Microgranite|35921|6|Mentioned|p38|||||||||
27682|Prestwood Microgranite|36216|1|Redefined|p213|Carboniferous|Carboniferous|||||||
27682|Prestwood Microgranite|37570|6|Mentioned|p122|||||||||
27682|Prestwood Microgranite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
27682|Prestwood Microgranite|39445|5|Briefly described|Table 12|||||||||
27682|Prestwood Microgranite|39687|6|Mentioned|Fig.5|||||||||
27682|Prestwood Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27682|Prestwood Microgranite|42547|5|Briefly described|p75|||||||||
27682|Prestwood Microgranite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
27682|Prestwood Microgranite|43740|4|Described|p22|||||||||
27682|Prestwood Microgranite|44047|14|Not recorded|Map Legend||Permian|||||||
27682|Prestwood Microgranite|44059|14|Not recorded|p442(Tb)||Late Paleozoic|||||||07-NOV-08
27682|Prestwood Microgranite|44516|2|Defined|p35,36||Late Paleozoic|Intrudes Etheridge Formation and Forsayth Granite.||||||07-NOV-08
27682|Prestwood Microgranite|45009|14|Not recorded|p75,Tb.13,15,Pl.13|||Possibly part of Esmeralda Granite intrusion. Intrudes Cumberland Range Volcanics.||||||
27682|Prestwood Microgranite|45014|2|Defined|p57,59,93,97,121-2,|Permian|Carboniferous|Pl.38,Tb.1.||||||
27682|Prestwood Microgranite|45087|5|Briefly described|p46|||Chemical analyses||||||
27682|Prestwood Microgranite|45113|6|Mentioned|p6|||Also mentioned P9.||||||
27682|Prestwood Microgranite|46845|6|Mentioned|Table 1|||||||||
27682|Prestwood Microgranite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Porphyritic biotite microgranite.||||||01-JUL-04
27682|Prestwood Microgranite|60081|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Grey porphyritic biotite microgranite.||||||
27682|Prestwood Microgranite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province.|||||Pinkish-grey to pink, abundantly porphyritic biotite microgranite.|
27682|Prestwood Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Cumberland Range Volcanic Group.|||||Biotite microgranite to rhyolite. I-type.|
75610|Pretty Bend Quartz Monzodiorite|68901|5|Briefly described|p4, p50-p53, p145|Early Cretaceous|Early Cretaceous|northern New England Orogen, Bowen Region. Forms scattered outcrops in the bed of the Don River.SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail. Younger K-Ar ages, 134+/-1 Ma and 142+/-3 Ma also mentioned.|142.9 +/- 1.1 Ma (SHRIMP U-Pb)||||Dark-grey, fine- to medium-grained, slightly porphyritic hornblende-clinopyroxene-biotite quartz monzodiorite.|15-NOV-18
75610|Pretty Bend Quartz Monzodiorite|69594|5|Briefly described|p565, p567, p571 Fig.7.46|Early Cretaceous|Early Cretaceous|Urannah Batholith. Forms scattered pavements in the bed of the Don River. Geochemistry plots. Three other ages are given.|142.9 +/- 1.1 Ma (SHRIMP: Cross et al., 2012).||||Commonly shows evidence of deformation: bent mica flakes, undulose extinction and partial recrystallisation in quartz grains, and well-developed foliation (highly attenuated mafic inclusions).|
36280|Pretty Swamp Rhyolite|23291|4|Described|p93 Fig. 3.9|Early Permian|Late Carboniferous|See also Pretty Swamp rhyolite. Parent: Bulleringa Volcanic Subgroup. Age: 289+/-2Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36280|Pretty Swamp Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Bulleringa Volcanic Subgroup, Scardons Volcanic Group.||||||
22698|Prices Cattle Creek Granodiorite|43259|6|Mentioned|Appendix 1,p50.|Early Devonian|Late Silurian|||||||
22698|Prices Cattle Creek Granodiorite|62521|6|Mentioned|p19|||Of Hartley and others (1989). ||||||
29324|Prices Dam Igneous Complex|23423|6|Mentioned|p258|||||||||
29324|Prices Dam Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 479. Assumed to be I-Type.||||||
29324|Prices Dam Igneous Complex|23713|5|Briefly described|p73 Appendix 2|||Intrudes Kitoba Member of the Hodgkinson Formation||||||
29324|Prices Dam Igneous Complex|43087|2|Defined|p94|Early Permian|Late Carboniferous|||||||
29324|Prices Dam Igneous Complex|43254|5|Briefly described|map legend|Early Permian|Late Carboniferous|Age Late Carboniferous to Early Permian? Of Almaden Supersuite.||||||
29324|Prices Dam Igneous Complex|43259|4|Described|Appendix 1,p50.|Permian|Carboniferous|||||||
29324|Prices Dam Igneous Complex|43285|5|Briefly described|Map Legend|||age Late Carboniferous-Early Permian?||||||
29324|Prices Dam Igneous Complex|43625|5|Briefly described|p61|||||||||
29324|Prices Dam Igneous Complex|60425|3|Fully described|p76, p108, p280-1 Appdx. |Early Permian|Late Carboniferous|Of Retire Suite and Almaden Suite (Almaden Supersuite) - rocks assigned to two suites? Comprises several small intrusions - 3 granite types are described on p281 - considerable lithology included (p281 and 283 Appdx.).||||||07-FEB-11
23920|Princess Hills Granite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||14-APR-15
23920|Princess Hills Granite|23424|5|Briefly described|Table 8.1||Carboniferous|Intrudes Kangaroo Hills Formation and Wairuna Formation.||||||
23920|Princess Hills Granite|23431|5|Briefly described|p541|||Kennedy Province||||||
23920|Princess Hills Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 405. I-Type.||||||
23920|Princess Hills Granite|23617|4|Described|Table 2 p18|||Also see p33. Intrudes Kangaroo Hills Formation. Kennedy Province.||||||
23920|Princess Hills Granite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
23920|Princess Hills Granite|23619|4|Described|p38 Table 2|Permian|Carboniferous|Intrudes Halls Reward Metamorphics, Wairuna Formation and Kangaroo Hills Formation. Herbert River Batholith Province.||||||
23920|Princess Hills Granite|42692|5|Briefly described|map legend|Carboniferous||||||||
23920|Princess Hills Granite|43113|4|Described|Table 2 p24|Permian|Carboniferous|||||||
23920|Princess Hills Granite|43253|5|Briefly described|map legend|Permian|Carboniferous|||||||
23920|Princess Hills Granite|43259|4|Described|Appendix 1,p45.|Permian|Carboniferous|||||||
40133|Princhester Serpentinite|24615|5|Briefly described|CD|Paleozoic|Neoproterozoic|[PLPzsp].  Serpentinite, serpentinised harzburgite, altered gabbro, minor pyroxenite.||||||07-NOV-08
40133|Princhester Serpentinite|50209|5|Briefly described|Map Legend|Paleozoic|Neoproterozoic|||||||07-NOV-08
40133|Princhester Serpentinite|50213|5|Briefly described|Map legend|||Age is Neoproterozoic or Palaeozoic. Serpentinite, serpentinised harzburgite, altered gabbro, minor pyroxenite.||||||28-MAY-08
40133|Princhester Serpentinite|60481|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|Sheared serpentinite, serpentinised harzburgite and minor dunite; minor lherzolite, pyroxenite, altered gabbro and dolerite, chromite, actinolite, quartzite.||||||07-NOV-08
40133|Princhester Serpentinite|60557|5|Briefly described|p17, p19 Fig. 5b|Early Paleozoic|Neoproterozoic|Ultramafic rocks. Age: 562+/-22Ma. See also p20 Fig. 5c.||||||07-NOV-08
40133|Princhester Serpentinite|61035|5|Briefly described|p16, p17, p24, p25, p34|Paleozoic|Paleozoic|Consists of thrust-imbricated slices of an ultramafic-mafic complex, in the Marlborough Block. Geological Province: Wandilla. Hosts Large Lode, Nine Mile Creek, Black Lade and Racecourse deposits.||||||07-FEB-11
40133|Princhester Serpentinite|63600|4|Described|p900, p914|Paleozoic|Neoproterozoic|A varied assemblage of metabasalts and metagabbros including Neoproterozoic rocks with mid-ocean ridge basalt. Referred to as Princhester ophiolite in this study - interpreted to be the mantle tectonite section of a dismembered ophiolite. See also p919.||||||07-FEB-11
40133|Princhester Serpentinite|65388|4|Described|p154-157, p70, 151, p224 Fig78, p427|Late Neoproterozoic|Late Neoproterozoic|Marlborough Block. Regarded as the basal component of an ophiolite, crops out over 580km2 as several sinuous belts, roughly rectangular area that extends from near Marlborough in the north-west to Canoona in the south-east. No type locality is assigned.  Sm/Nd isochron crystallisation age: 562+/- 22 Ma. Emplacement on continental margin ~Late Devonian. Imbricated thrust slices in contact with Marlborough Metamorphics. Intruded by Cleethorpes Granodiorite and Racecourse Gabbro. In faulted contact with Rookwood Volcanics. 95% serpentinised mantle peridotite; chromitite, metagabbro, metamorphosed mafic dykes.||||||08-SEP-14
40133|Princhester Serpentinite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Contains dolerite and gabbro pods attributed to the c.575 Ma Skipworth Event, ME 29 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.575 Ma.|||||
40133|Princhester Serpentinite|68008|3|Fully described|p7-8, p19, p21, p174, p292, p296|Cambrian|Neoproterozoic|See also p303-307, p340, p484, p487-489. Described by Murray (1969), but the name is from Harbort (2001): one of several names he applied to serpentinites in various thrust sheets in the area. They are all combined under this name for simplicity. Oldest rock in the Yarrol Province. Originally the mantle component of a spreading centre ophiolite. No type locality. Crops out as sharp-crested ridges. Geochemistry discussed: REE and spidergram plots. Structure detailed. Forms the Marlborough Block: alternating slices with Marlborough Metamorphics. Has lateritic weathering profiles containing chrysoprase, magnetite and Ni-Co ore. Hosts minor chromite and magnesite. Ophiolite generation dated at 380 +/- 19 Ma.|562 +/- 22 Ma (protolith).|||Is thrust over Berserker and Rockhampton Groups, Craigilee beds, Mount Alma Formation. Is intruded by Wattlebank Granodiorite.|Mostly serpentinised mantle peridotite, from a dominant tectonite harzburgite protolith; mainly massive, locally schistose. Scattered small chromite bodies, generally massive and podiform. A variety of mafic inclusions and dykes.|
40133|Princhester Serpentinite|68359|6|Mentioned|p9|||||||||
40133|Princhester Serpentinite|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Marlborough Province.||||||
40133|Princhester Serpentinite|68679|5|Briefly described|p308-312, p347, p426|Neoproterozoic|Neoproterozoic|Withnall et al. (2009). Marlborough Block, northern New England Orogen. Outcrop area ~600 kms. Forms several sinuous belts between Marlborough and Canoona. Ultramafic-mafic imbricate thrust slices. Regarded as the basal component of an ophiolite. Lithologies described in detail.|562 +/- 22 Ma (Sm-Nd: Bruce et al., 2000).|||Imbricated with Marlborough Metamorphics. Is intruded by Cleethorpes and Wattlebank Granodiorites and Racecourse Creek Gabbro.|Four thrust sheets dominated by serpentinised peridotite, with serpentinised harzburgite with minor dunite and pyroxenite, podiform chromitite, gabbro and various basaltic intrusions.|
40133|Princhester Serpentinite|69952|6|Mentioned|p75|Paleozoic|Neoproterozoic|||||||
40133|Princhester Serpentinite|72297|5|Briefly described|p732, p757|||Associated with QLD's major magnesite deposits, formed by CO2-charged groundwater reacting with this unit. Other, minor deposits listed. Weathering produces nickeliferous laterite, associated with chrysoprase in the Marlborough Province, ~90km NW of Rockhampton.||||||
40133|Princhester Serpentinite|73197|6|Mentioned|p473|||New England Orogen, northern. Marlborough Block. Interpreted as a remnant of partially melted upper mantle peridotite from an oceanic spreading centre, later interacted with magmas in a Devonian island arc (Murray, 2007).||||||
81238|Prize 1|66844|6|Mentioned|p264|||||Of Prize Supersequence. Included within lower McNamara Group.||||
81239|Prize 2|66844|4|Described|p243, p254, p255-257, p260-265, 273.|||Torpedo Creek-Lower Gunpowder Creek Depositional Sequence (Prize 2.1-2.3). Transgressive systems tract overlain by highstand systems tract. Details of fourth order sequences in Table 2 p260, 263. Lawn Hill Platform. Syn-depositional siliciclastic storm-ramp sediments deposited in locally fault-controlled (e.g. Kamarga Dome, Mount Gordon Fault Zone) depocentres. Overall thickness is highly variable due to segmentation by block faulting; local sediment sources and depocentres. Characterised by 4 stacked shallowing upwards sequences (see p246-251 for detailed lithofacies descriptions). Subdivided into 3 fourth-order sequences (Prize 2.1-2.3); refer to p247-250, 255-263 for detailed illustrations and further definitions and criteria. Deposition was terminated by Gun Supersequence boundary; 28my depositional hiatus and erosional surface. See p264-265 for sequence stratigraphic analysis.||Of Prize Supersequence. Included within lower McNamara Group.|Prize 2.1 to Prize 2.3 fourth order sequences.|Overlain by Gun Supersequence.||
40571|Prize Supersequence|62535|5|Briefly described|p663, p672-674|||Calvert Superbasin. Time-equivalent to the ~1695-1685 Ma Broken Hill Group. Thickness varies up to 1500m. Deposition was followed by a 15-20 m.y. hiatus.|c.1695? Ma - c.1690 Ma.|||Unconformably overlies Big Supersequence. Is overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|63112|6|Mentioned|p1191 Fig.2|||Calvert Superbasin.||||||
40571|Prize Supersequence|63866|5|Briefly described|p53-p54, p56, p58, p61-p62|||Calvert Superbasin. Magmatism in the Leichhardt River Fault trough initiated at 1690 and is expressed as peprites within stratigraphic units of this supersequence.|||Includes the Wunummantyala Sandstone, Aquarium Fomration, Wollogorang Formation, Packsaddle Granite, Hobblechain Rhyolite, Tanumbirini Rhyolite and Nyanantu Formation.|Equivalent to the Fish River Formation.||
40571|Prize Supersequence|65228|5|Briefly described|p21, p25, Fig.10.|||Calvert Superbasin. Gamma ray log, lithology and facies detailed.||||||
40571|Prize Supersequence|65337|6|Mentioned|p32.|||This study includes a younger  (<1700 Ma) component of Surprise Creek Formation in this Supersequence.||||Is overlain by Gun Supersequence.||
40571|Prize Supersequence|66844|4|Described|p243-245,254, 264, 265|||Lawn Hill Platform. Lower suite of fault-bounded, storm dominated siliclastic ramps.  Separated from the overlying Gun SS by a regionally correlative unconformity in the lower to middle Gunpowder Creek Formation. Shown as Prize Sequence on p264.||Equivalent to parts of lower McNamara Group.|Divided into Prize 1 and Prize 2 (p254) depositional sequences.|Overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also p13, p15, p39. Leichhardt River Domain, Mount Isa Inlier. Unconformity at base.|~1705-1680 Ma.|||Overlies Big Supersequence. Is overlain by Gun Supersequence. Equated with the Knapdale Quartzite.||
40571|Prize Supersequence|67539|6|Mentioned|p3|||||||||
40571|Prize Supersequence|68021|5|Briefly described|p135 Fig 4, p136, 137 Fig 5|Statherian|Statherian|Calvert Superbasin. Environment changing from near-shore to deltaic or shallow marine. |~1790 - ~1785 Ma|||Equivalent to Surprise Creek Formation.|Several cycles of upward-fining mainly siliciclastic sedimentation, followed by increasing amounts of thinly laminated carbonaceous shale or rhythmite.|
40571|Prize Supersequence|68146|5|Briefly described|p194, p199-200|||Magmatism started with Sybella-aged peperites at c.1690 Ma and lasted until emplacement of the Queen Elizabeth pluton at c.1655 Ma.|||Lower part of Torpedo Creek and Warrina Park Quartzites.|Is overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|68575|6|Mentioned|p40|||||||||
40571|Prize Supersequence|68732|5|Briefly described|p159, p161, p162, p166-169, p171|||Includes lower Gunpowder Creek Formation, Surprise Creek Formation, Warrina Park Quartzite, Deighton Quartzite (units 1-4), Knapdale Quartzite, Roxmere  Quartzite, Doherty Formation. Contains pink cherty beds with a detrital zircon age of ca 1690 Ma.|||||Comprises a full suite of shelfal siliclastic facies.|
40571|Prize Supersequence|69056|6|Mentioned|p54|||Calvert Superbasin.||||Equivalent to Knapdale Quartzite.||
40571|Prize Supersequence|69591|5|Briefly described|p27, p37-40, p54|||Mount Isa Province. Includes the Surprise Creek Formation, Stanbroke Sandstone and Knapdale Quartzite.||||Correlated with middle unit of Deighton Quartzite.||
40571|Prize Supersequence|70657|6|Mentioned|p17|||||||||
40571|Prize Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill. Intruded by the Sybella Batholith.|ca. 1700 Ma|||Overlies the Fiery Creek Volcanics.|Sandstone and greywacke.|
40571|Prize Supersequence|73144|4|Described|p9-10, p29|Statherian|Statherian|Sequence Stratigraphy. Calvert Superbasin. Deposited in a coastal plain, nearshore environment with some below storm wavebase deposits (Southgate et al., 2000). Consists of a basal sandstone that dirties upwards to deeper water siltstone and black shales.|1690-1705 Ma|||Includes Surprise Creek Formation and Warrina Park Quarzite, Torpedo Creek Quartzite, and the lower Gunpowder Creek Formation.|Sandstone, conglomerate and siltstone.|
36293|Promise Creek Granite|23291|5|Briefly described|p97 Tb 3.11|||Geological Province: Georgetown Region.||||||08-JUL-15
36293|Promise Creek Granite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36293|Promise Creek Granite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Kangaroo Creek Supersuite.||||
30147|Puckley Suite|43098|6|Mentioned|p35|||Of Cape Melville Supersuite.||||||03-JUN-09
30147|Puckley Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Yates Supersuite. Contains Puckley and Leichhardt Pocket Granites. I-types.||||||07-FEB-11
23922|Puddler Creek Formation|22611|6|Mentioned|P191||Cambrian|||||||
23922|Puddler Creek Formation|22621|5|Briefly described|p204|Ordovician|Cambrian|part of Seventy Mile Range Group||||||
23922|Puddler Creek Formation|22675|6|Mentioned|p13|||||||||
23922|Puddler Creek Formation|22847|5|Briefly described|p 7|||Seventy Mile Range Group||||||
23922|Puddler Creek Formation|23278|5|Briefly described|Fig1p81||Cambrian|||||||
23922|Puddler Creek Formation|23318|4|Described|p392 Fig.2|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Sandstone and greywacke; alkali basalt and trachyandesite lavas and sills.||||||07-FEB-07
23922|Puddler Creek Formation|23422|4|Described|p170, p206 Table 6.3|Middle Ordovician|Cambrian|Of Seventy Mile Range Group.  Overlying unit: Mount Windsor Volcanics.||||||
23922|Puddler Creek Formation|23430|4|Described|p469-470.|||Of Seventy Mile Range Group. Overlying Unit Mount Windsor Volcanics - conformable. Thalanga Province.||||||
23922|Puddler Creek Formation|23431|5|Briefly described|p537|||||||||
23922|Puddler Creek Formation|23505|5|Briefly described|Map legend|Ordovician|Cambrian|of Seventy Mile Range Group.||||||
23922|Puddler Creek Formation|23764|5|Briefly described|p340|Cambrian|Cambrian|Sandstone, siltstone, minor andesite and dolerite.   Parent: Seventy Mile Range Group.||||||
23922|Puddler Creek Formation|23852|5|Briefly described|p816|Cambrian|Cambrian|Of Seventy Mile Range Group. Overlying Unit Mount Windsor Formation.||||||
23922|Puddler Creek Formation|23893|5|Briefly described|p12||Late Cambrian|Of Seventy Mile Range Group.||||||
23922|Puddler Creek Formation|23940|5|Briefly described|p917 Fig. 3|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group.  Formation is Fm. in text.  Geological Province: Mount Windsor subprovince.||||||
23922|Puddler Creek Formation|23950|5|Briefly described|p1134 Fig.1|Cambrian|Cambrian|Of the Seventy Mile Range Group. Conformably overlain by the Mount Windsor Formation.||||||
23922|Puddler Creek Formation|23952|4|Described|p1176 Fig.1|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Conformably overlain by the Mount Windsor Formation. Geological Province: Mount Windsor subprovince||||||
23922|Puddler Creek Formation|23953|5|Briefly described|p1202 Fig.1|Ordovician|Cambrian|Geological Province: Mount Windsor subprovince||||||
23922|Puddler Creek Formation|23954|5|Briefly described|p1227|||Max. Thickness: 9km.||||||
23922|Puddler Creek Formation|23988|5|Briefly described|p15|Cambrian|Cambrian|Of Seventy Mile Range Group.||||||
23922|Puddler Creek Formation|24035|5|Briefly described|p3 Fig. 1|Cambrian|Cambrian|Of Seventy Mile Range Group. Micaceous sandstone, siltstone.||||||
23922|Puddler Creek Formation|24424|4|Described|p524|Late Cambrian|Late Cambrian|Of 70 Mile Group. Siltstones, sandstones and greywackes, metamorphosed to greenschist facies. See also Puddler Creek Metasediments. Geological Province: Lolworth-Ravenswood Province.||||||
23922|Puddler Creek Formation|37765|5|Briefly described|p9|||||||||
23922|Puddler Creek Formation|38658|6|Mentioned|p152|||||||||
23922|Puddler Creek Formation|39445|6|Mentioned|p66|||||||||
23922|Puddler Creek Formation|40746|3|Fully described|p345|||Mention Fig.2||||||
23922|Puddler Creek Formation|41806|6|Mentioned|p45|||||||||
23922|Puddler Creek Formation|42279|5|Briefly described|p27|||||||||
23922|Puddler Creek Formation|42288|5|Briefly described|p25|||||||||
23922|Puddler Creek Formation|42633|4|Described|p14|||||||||
23922|Puddler Creek Formation|42750|6|Mentioned|p36|||||||||
23922|Puddler Creek Formation|43093|5|Briefly described|p13|||of Seventy Mile Range Group||||||
23922|Puddler Creek Formation|43109|6|Mentioned|p68|||||||||
23922|Puddler Creek Formation|43128|5|Briefly described|Fig.6,p476|||||||||
23922|Puddler Creek Formation|43259|6|Mentioned|Appendix 1,p7.|Ordovician|Cambrian|Upper Cambrian - Lower Ordovician in age.||||||03-DEC-13
23922|Puddler Creek Formation|43763|4|Described|p740|Late Cambrian|Middle Cambrian|||||||
23922|Puddler Creek Formation|43773|5|Briefly described|Fig.1,p765|||||||||
23922|Puddler Creek Formation|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23922|Puddler Creek Formation|62077|5|Briefly described|p34, p35 Fig.1, p37 Fig.2|Ordovician|Cambrian|Appears as Puddler Creek metasediments in Fig.2.||||Is intruded by Fenian Granite.|Metasediments.|
23922|Puddler Creek Formation|62470|5|Briefly described|p181 Fig. 1|Ordovician|Cambrian|Basal unit of the Seventy Mile Range Group. Volcanic (basalt and andesite)-sedimentary package dominated by quartz and lithic sandstone, feldspar-quartz-lithic sandstone, and siltstone. Overlain by Mount Windsor Formation. Max. thickness: 9000m.||||||07-FEB-11
23922|Puddler Creek Formation|68731|5|Briefly described|p128, p145, p146|Early Ordovician|Early Ordovician|Henderson (1986); Beams and Hartley (1990); Berry et al. (1992). Contributes more than half of the Seventy Mile Range Group. The Kirk River Beds is a possible outlier of the Puddler Creek Formation. Age constrained by the Seventy Mile Range Group.||Lowermost unit of the Seventy Mile Range Group.||Possible correlative of the Les Jumelles beds.|Comprises fine-grained, micaceous, continentally derived siltstone, sandstone, and greywacke intruded by numerous mafic dykes.|
23922|Puddler Creek Formation|68900|5|Briefly described|p12, p18|Early Ordovician|Cambrian|||Seventy Mile Range Group||Conformably overlain by the Mount Windsor Volcanics.||
23922|Puddler Creek Formation|69952|5|Briefly described|p4, p108, p110|||Charters Towers Province. Lithologically similar to Les Jumelles beds to the S. Maximum depositional age. Inferred to be Cambrian: its minimum age of 479 +/- 5 Ma is of the overlying unit, Mount Windsor Volcanics.|c.499 Ma (unpublished data).|Basal unit in Seventy Mile Range Group.||Is overlain by Mount Windsor Volcanics. Is correlated with Les Jumelles beds.||30-NOV-15
23922|Puddler Creek Formation|70033|5|Briefly described|p4|||Thomson Orogen. Maximum depositional age: mid- to late Cambrian.||Seventy Mile Range Group.||||
23922|Puddler Creek Formation|70207|6|Mentioned|p38-39|||A lithic sandstone with a maximum depositional age of 498.7 +/- 5.8 Ma, thought to be from the Mount Windsor Volcanics, may be from this unit. Collected from Britannia Station ~33km S of Charters Towers.||||||
23922|Puddler Creek Formation|70740|6|Mentioned|p20|||Possible correlative of the Les Jumelles beds.||Seventy Mile Range Group||||
23922|Puddler Creek Formation|71592|5|Briefly described|Appendix A.|||Charters Towers Province, Thomson Orogen.|499+/-5.8 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
36154|Puddler Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Cambrian|||||||
24464|Puppy Camp Granodiorite|23291|4|Described|p89 Fig. 3.8|||Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
24464|Puppy Camp Granodiorite|23430|5|Briefly described|p486|||||||||
24464|Puppy Camp Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 55. Assumed to be I-Type.||||||
24464|Puppy Camp Granodiorite|23619|4|Described|p40 Table 2|Early Devonian|Silurian|Intrudes Einasleigh Metamorphics. Also see p7. Overlying unit Newcastle Range Volcanic Group. Georgetown Province.||||||
24464|Puppy Camp Granodiorite|39981|2|Defined|p105|Devonian|Silurian|Silurian-Devonian||||||
24464|Puppy Camp Granodiorite|40542|6|Mentioned|p98|||||||||
24464|Puppy Camp Granodiorite|41680|3|Fully described|p125|||||||||
24464|Puppy Camp Granodiorite|43113|4|Described|Table 2 p26|Early Devonian|Silurian|||||||
24464|Puppy Camp Granodiorite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24464|Puppy Camp Granodiorite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
24464|Puppy Camp Granodiorite|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Muscovite-biotite and biotite granodiorite.||||||
24464|Puppy Camp Granodiorite|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Pale grey equigranular to slightly porphyritic muscovite-biotite and biotite granodiorite.|
24464|Puppy Camp Granodiorite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
23926|Puranga Rhyolite|23291|4|Described|p92 Fig. 3.9|Early Permian|Late Carboniferous|Parent: Maureen Volcanic Group. Age: uncertain. Thickness: 200-480m. Geological Province: Georgetown Region.||||||19-MAY-15
23926|Puranga Rhyolite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Maureen Volcanic Group.||||||
23926|Puranga Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V7. Assumed to be I-Type.||||||
23926|Puranga Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23926|Puranga Rhyolite|40542|6|Mentioned|p97|||||||||
23926|Puranga Rhyolite|43259|4|Described|Appendix 1,p1.||Carboniferous|of Maureen Volcanic Group.||||||
23926|Puranga Rhyolite|50595|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Maureen Volcanic Group. Overlies: Womblealla Rhyolite Member.||||||01-JUL-04
23926|Puranga Rhyolite|68352|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Maureen Cauldron. Min Age: Early Permian?||Unit in Maureen Volcanic Group.||Conformably overlies Womblealla Rhyolite Member.|Polymictic rhyolitic volcanic breccia, locally intrusive; crystal-poor rhyolitic ignimbrite and breccia; very fine-grained shard-rich rhyolitic ignimbrite with prominent large quartz and K-feldspar crystals in basal part.|18-MAY-15
25420|Purkin Granite|23032|6|Mentioned|p45,46|Silesian||K/Ar Age: 311+/-5Ma (probably a minimum age).||||||
25420|Purkin Granite|23220|5|Briefly described|Fig.2|Permian|Carboniferous|K/Ar age 305Ma. Intrudes Einasleigh Metamorphics. Correlate of Elizabeth Creek Granitic Suite.||||||
25420|Purkin Granite|23291|4|Described|p50, p98 Tb. 3.11|Late Carboniferous|Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
25420|Purkin Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 46. I-Type.||||||
25420|Purkin Granite|35920|1|Redefined|p26|Carboniferous|Carboniferous|||||||
25420|Purkin Granite|37576|5|Briefly described|p8|||||||||
25420|Purkin Granite|38715|6|Mentioned|p192|||||||||
25420|Purkin Granite|39445|5|Briefly described|Table 12|||See also P90||||||
25420|Purkin Granite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25420|Purkin Granite|43259|4|Described|Appendix 1,p18.||Carboniferous|||||||
25420|Purkin Granite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
25420|Purkin Granite|43603|5|Briefly described|p6||Carboniferous|||||||
25420|Purkin Granite|43664|6|Mentioned|p96|||||||||
25420|Purkin Granite|43740|3|Fully described|p31||Carboniferous|||||||
25420|Purkin Granite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
25420|Purkin Granite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Gray to pink medium to coarse-grained biotite granite and grey porphyritic biotite microgranite.||||||17-MAY-04
25420|Purkin Granite|64707|5|Briefly described|Map legend|Carboniferous|Carboniferous|Grey to pink, medium- to coarse-grained biotite granite, and grey porphyritic biotite microgranite.||||||
25420|Purkin Granite|68338|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province.|||||Grey to pink, medium- to coarse-grained biotite granite, and grey porphyritic biotite microgranite.|
25420|Purkin Granite|68357|5|Briefly described|Map legend.|Carboniferous|Carboniferous|Kennedy Province.|||||Grey to pink, medium- to coarse-grained biotite granite and grey porphyritic biotite microgranite.|
25420|Purkin Granite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous||||||Grey to pink, medium to coarse-grained biotite granite and grey porphyritic biotite microgranite.|
25420|Purkin Granite|69593|5|Briefly described|p489, p511|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|330 Ma.||||I-type.|
23928|Puzzler Granodiorite|22847|3|Fully described|p 45|Ordovician|Ordovician|||||||
23928|Puzzler Granodiorite|22937|5|Briefly described|fig2 p2o6||Devonian|||||||
23928|Puzzler Granodiorite|23422|6|Mentioned|p210 Table 6.6|||||||||
23928|Puzzler Granodiorite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
23928|Puzzler Granodiorite|42750|2|Defined|p37||Ordovician|||||||
23928|Puzzler Granodiorite|43093|4|Described|Appendix 1||Ordovician|Middle Ordovician age.||||||
23928|Puzzler Granodiorite|43687|6|Mentioned|Fig.2,p205|||||||||
23928|Puzzler Granodiorite|43933|5|Briefly described|Map Legend||Ordovician|||||||
23928|Puzzler Granodiorite|62521|6|Mentioned|p16|||Similar to Columbia Creek Complex granites.||||||
34774|Puzzler Walls group|22937|6|Mentioned|p206|||Informal name.||||||
27979|Pyramid Rhyolite|22675|4|Described|p53|||Bulgonunna Volcanic Group||||||
27979|Pyramid Rhyolite|43391|5|Briefly described|Map legend||Late Carboniferous|Of the Bulgonunna Volcanic Group.  Geological Province: Coastal Ranges Igneous Province.||||||23-JUN-04
27979|Pyramid Rhyolite|43727|5|Briefly described|Table 14,p50|||||||||
27979|Pyramid Rhyolite|60659|5|Briefly described|p16|||Of the Bulgonunna Volcanic Group. A lower moderately crystal-rich unwelded or very poorly welded ignimbrite and an upper moderately crystal-rich welded ignimbrite. Part of the Locharwood association. Of the Bulgonunna Province.||||||07-FEB-11
27979|Pyramid Rhyolite|64852|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Bulgonumma (sic) Volcanic Group - place name is actually spelt as Bulgonunna. Mainly purple, moderately crystal-rich rhyolitic ignimbrite.||||||10-FEB-09
27979|Pyramid Rhyolite|67874|6|Mentioned|p49|||Mentioned in analytical session metadata.||||||
27979|Pyramid Rhyolite|68679|5|Briefly described|p362|Permian|Pennsylvanian|Kennedy Igneous Association.|302.4 +/- 2 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
27979|Pyramid Rhyolite|68900|6|Mentioned|p30|||||||||
27979|Pyramid Rhyolite|68901|4|Described|p5, p114-p116, p144|||Kennedy Igneous Association, Thomson Region. Crops out in several bodies between the Pyramid Range and Reginald Peak. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|302.4 +/- 2.0 Ma(SHRIMP U-Pb)|Bulgonunna Volcanic Group||Overlies the Mount Wyatt and Saint Anns Formations. Equivalent to the Locharwood Rhyolite.|Welded and non-welded ignimbrite. Pumice-rich, welded rhyolitic ignimbrite.|27-SEP-18
27979|Pyramid Rhyolite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
27979|Pyramid Rhyolite|70740|5|Briefly described|p8, p35, p82 fig 50, p88|Late Carboniferous|Late Carboniferous|SHRIMP age derived from Cross et al, 2012. |302.4 +/- 2.1 (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Overlies the Saint Anns Formation, Bimurra Volcanics. Overlain by the Hidden Valley Rhyolite.|Altered, pumice-rich rhyolitic ignimbrite. Includes lower nonwelded and upper welded parts.|
27979|Pyramid Rhyolite|71592|5|Briefly described|Appendix A.|||Drummond Basin.|302+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
26115|Pyri Pyri Granite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
26115|Pyri Pyri Granite|31659|2|Defined|p91|Cretaceous|Cretaceous|Prob. Cretaceous||||||
26115|Pyri Pyri Granite|32357|3|Fully described|p8|||Table 2||||||
26115|Pyri Pyri Granite|32361|6|Mentioned|Map legend|Cretaceous|Permian|Perm. or Cret.||||||
26115|Pyri Pyri Granite|38081|5|Briefly described|Table 2|||||||||
26115|Pyri Pyri Granite|39445|5|Briefly described|Table 12|||||||||
26115|Pyri Pyri Granite|41246|6|Mentioned|Map legend|Cretaceous|Permian|||||||
26115|Pyri Pyri Granite|41922|4|Described|Table 2, P12|||||||||
26115|Pyri Pyri Granite|42660|4|Described|p23 p167|||||||||
26115|Pyri Pyri Granite|61035|5|Briefly described|p18, p19, p21|||Intrudes Double Mountain Volcanics. Unit defined by Kirkegaard + others (1970). Consists of muscovite-biotite granite, biotite + hornblende granite, minor biotite-hornblende granodiorite. Unit outcrop well exposed in th Normandy Ranges.||||||07-FEB-11
26115|Pyri Pyri Granite|65388|6|Mentioned|p70 Fig. 28, p226|||Permian to Triassic? Overlain by Herbert beds?||||||
26115|Pyri Pyri Granite|68679|5|Briefly described|p308, p410, p423-424, p426-427|||Yarrol Province. A large unit (285 km2); a complex of intrusions NE of the Yarrol Belt between Pyri Pyri and Mount Mulgrave. Age uncertain; has been given as Permian to Cretaceous.|269.3 +/- 3 Ma (Cross, unpub.).|||Intrudes Double Mountain Volcanics and Wandilla Formation.|Muscovite-biotite granite, hornblende-biotite granite, biotite-hornblende granodiorite, porphyritic dacite.|
26115|Pyri Pyri Granite|69599|6|Mentioned|p589|||Thought to constitute the eastern edge of the Herbert Creek Basin.||||||
26115|Pyri Pyri Granite|69952|5|Briefly described|p73, p75|Permian|Permian|New England Orogen. A mid-Permian age is inferred from latest age determinations of nearby Mailmans Gap Granodiorite.||||||23-NOV-15
36165|Python Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36165|Python Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 264. I-Type.||||||
36165|Python Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36165|Python Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, medium-grained, porphyritic biotite granite; alteration zones common. I-type.||||||07-FEB-11
23929|Quadroy Conglomerate|23076|6|Mentioned|p724|||||||||
23929|Quadroy Conglomerate|23423|4|Described|p301 Table 7.2|Early Carboniferous|Late Devonian|Also see p234. Hodgkinson Province||||||
23929|Quadroy Conglomerate|23430|4|Described|p511-512|||Also see p471. Hodgkinson Province.||||||
23929|Quadroy Conglomerate|23431|6|Mentioned|p539|||Hodgkinson Province.||||||
23929|Quadroy Conglomerate|23500|5|Briefly described|Map legend|||Age: Late Devonian? - Early Carboniferous? Hodgkinson Province.||||||
23929|Quadroy Conglomerate|23616|4|Described|Table 1C p13, p37|Early Carboniferous|Late Devonian|Faulted against Dargalong Inlier, Mulgrave Fm, and locally against Chillagoe Fm. Locally unconformably overlies Chillagoe Fm. Age: Late Devonian? or E. Carboniferous. Younger than Hodgkinson and Chillagoe Fms. Hodgkinson Province.||||||
23929|Quadroy Conglomerate|23713|4|Described|p15|Early Carboniferous|Late Devonian|Hodgkinson Province.||||||
23929|Quadroy Conglomerate|24485|5|Briefly described|p1|Early Carboniferous|Late Devonian|Geological Province: Hodgkinson Province||||||
23929|Quadroy Conglomerate|24486|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Coarse polymictic conglomerate, conglomeratic feldspathic arenite, feldspathic arenite; minor sedimentary breccia.||||||
23929|Quadroy Conglomerate|24487|5|Briefly described|Map legend|||||||||
23929|Quadroy Conglomerate|40892|6|Mentioned|p74|||||||||
23929|Quadroy Conglomerate|41824|6|Mentioned|p201|||||||||
23929|Quadroy Conglomerate|42113|6|Mentioned|p259|||||||||
23929|Quadroy Conglomerate|42500|5|Briefly described|p11|||Used by Fawckner 1981.||||||
23929|Quadroy Conglomerate|42620|3|Fully described|p123|Early Carboniferous|Late Devonian|||||||
23929|Quadroy Conglomerate|43060|3|Fully described|p53,Table 1c|||probable Late Devonian or Early Carboniferous age.||||||
23929|Quadroy Conglomerate|43083|3|Fully described|p26, p70-72|Early Carboniferous|Late Devonian|Geological province: Hodgkinson Province. Mainly massive pebbly to bouldery arkose and conglomerate.||||||17-JUN-09
23929|Quadroy Conglomerate|43254|5|Briefly described|map legend|Early Carboniferous|Late Devonian|Of Hodgkinson Province.||||||
23929|Quadroy Conglomerate|43285|5|Briefly described|Map Legend|||age Late Devonian? to Early Carboniferous?||||||
23929|Quadroy Conglomerate|43625|3|Fully described|p19,33-34|||||||||
23929|Quadroy Conglomerate|44246|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
23929|Quadroy Conglomerate|60357|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Hodgkinson Province.||||||
23929|Quadroy Conglomerate|60425|3|Fully described|p13, p16 Tb. 1, p28-29|Early Carboniferous|Late Devonian|Faulted contact with Mulgrave Formation. Max. thickness: ~700m. Geological province: Hodgkinson Province.  Massive, coarse, polymictic conglomerate -- further lithological details included.||||||07-FEB-11
23929|Quadroy Conglomerate|62371|5|Briefly described|p472 Fig.3|Devonian|Devonian|||||||
23929|Quadroy Conglomerate|63140|6|Mentioned|p572 fig 3|Carboniferous|Devonian|Hodgkinson Province.||||||
23929|Quadroy Conglomerate|63154|5|Briefly described|p281 Fig. 3|Late Devonian|Late Devonian|Geological province: Hodgkinson Province. Age: ~360Ma.||||||11-APR-07
23929|Quadroy Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Mount Windsor Subprovince. This unit, as well as Mountain Creek Conglomerate, Van Dyke Litharenite and Mulgrave Formation, are all mapped under the symbol, Om.||||||
23929|Quadroy Conglomerate|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Chillagoe Subprovince, Hodgkinson Province.||||||
23929|Quadroy Conglomerate|69079|6|Mentioned|p3-4|||Hodgkinson Province.||||||
23929|Quadroy Conglomerate|69592|5|Briefly described|p230, p231 Fig.4.4, p242-243, p245, p297|Carboniferous|Carboniferous|Fawckner (1981). A distinctive, fault-bounded conglomerate unit cropping out as discontinuous lenses on the western margin of Hodgkinson Province, abutting the Palmerville Fault. High energy, probably proximal fan environment. Age is not determined.|||||Massive, unsorted to very poorly sorted, grain-supported pebble to boulder conglomerate (with generally rounded and mainly granite clasts); and locally pebbly, micaceous, feldspathic sandstone.|
23929|Quadroy Conglomerate|70207|6|Mentioned|p74|||Included in a group of units collectively aged as Ordovician-Silurian & Carboniferous?.||||||
23929|Quadroy Conglomerate|70345|6|Mentioned|p3|Carboniferous|Late Ordovician|||||||
23929|Quadroy Conglomerate|70673|6|Mentioned|p7|||Age (range) given as "Late Ordovician & Carboniferous?[sic]".||||||
23929|Quadroy Conglomerate|72983|6|Mentioned|p15|Carboniferous?|Ordovician|||||||
23929|Quadroy Conglomerate|73595|6|Mentioned|p1134|||Hodgkinson Province, Mossman Orogen.||||||
78952|Quaggy Mountain Gabbro|65388|3|Fully described|p330, 13, 301, 303, 304, 315, 327, 340|Late Permian |Late Permian |Intrudes Yerilla Metamorphics. Other contacts obscured by Cenozoic cover. Age inferred from similarities with Delubra Gabbro. Dark greenish grey gabbro, locally layered. Olivine gabbro to hornblende-pyroxene gabbro.||||||
78952|Quaggy Mountain Gabbro|68679|5|Briefly described|p419|Permian|Permian|Rawbelle Batholith. ~25 km2, but extent under cover probably greater. Permian age from similarity to Delubra Gabbro.||||Intrudes Yerilla Metamorphics.|Clinopyroxene-hornblende gabbro and olivine gabbro to diorite and quartz diorite; magnetite-rich; commonly layered.|
29321|Quaker Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29321|Quaker Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~303 Ma K-Ar. of Ootann Supersuite.||||||
29321|Quaker Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 331. I-Type.||||||
29321|Quaker Granite|23616|6|Mentioned|Table 6 p72|||Of Ootann Supersuite.||||||
29321|Quaker Granite|43060|5|Briefly described|Table 6|||of Ootann Supersuite||||||
29321|Quaker Granite|43083|5|Briefly described|p255|||Of Ootann Supersuite. Intrudes Ootann Granite? I-type. Lithology included.||||||30-MAR-15
29321|Quaker Granite|43087|2|Defined|p63|Late Carboniferous||Of Ootann Supersuite. Reserved as Quaker Adamellite.||||||
29321|Quaker Granite|43259|4|Described|Appendix 1,p39.||Late Carboniferous|||||||
29321|Quaker Granite|60425|4|Described|p278-9 Appdx, p283 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Age: 306+/-3Ma, 300+/-2Ma (K-Ar). I-type. Pale grey, fine-grained, slightly to moderately porphyritic (hornblende-) biotite granite; scattered mafic enclaves to ~75cm; most samples slightly to moderately altered.||||||30-MAR-15
29321|Quaker Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Two un-named sub-units are mapped separately; a leucocratic biotite monzogranite, locally miarolitic, which forms net-veined complex with Muldiva Granodiorite in places, and minor aplite; and a medium-grained leucocratic biotite-hornblende granodiorite, pervasively 'iron' stained. |300 +/- 2 Ma (K-Ar, biotite).|Unit in Ootann Supersuite.|||Pale grey, fine-grained, slightly to moderately porphyritic (hornblende-)biotite monzogranite to granodiorite; with scattered mafic enclaves to ~75 cm; slightly to moderately altered.|
40134|Quarry Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbq].  Dark grey to black medium-grained quartz-hornblende-biotite-hypersthene-augite gabbro.||||||
40134|Quarry Gabbro|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex.||||||
40134|Quarry Gabbro|68008|2|Defined|p357-359, p361, p621|Early Triassic|Permian|New unit. A small E-W trending intrusion 2.5km SE of Stanwell power station. Name derived from Quarry Creek. The type area is the semi-circle of hills surrounding the S end of the water storage dam for Stanwell power station, where excellent outcrops of boulders occur. These have been quarried as black granite for the building stone industry. Geophysics modelling.||Bouldercombe Igneous Complex.||Intrudes Capella Creek Group and Lorray Formation. Is overlain by Precipice Sandstone.|Dark grey to black, medium-grained gabbro. Plagioclase, as subhedral laths to 4mm long, comprises c.60% of the rock.|
40134|Quarry Gabbro|68679|5|Briefly described|p424, p426|||Yarrol Province. ~4.5 x 2.5km unit in the eastern lobe of the Complex; part of a gabbroic rim surrounding the core of Bundaleer Tonalite (relationship with that unit unknown).||Bouldercombe Igneous Complex.||Intrudes Capella Creek Group and Lorray Formation.|Quartz-biotite-hornblende-hypersthene-augite gabbro.|
36612|Quartz Hill granite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
36612|Quartz Hill granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 413.  I-Type.||||||
30701|Queen Elizabeth Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
30701|Queen Elizabeth Granite|23545|5|Briefly described|p606 Table 1.|||||||||
30701|Queen Elizabeth Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30701|Queen Elizabeth Granite|50536|5|Briefly described|p1.5, 8.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.  Age: 1660-1665 +/- 5Ma (Shrimp).||||||07-NOV-08
30701|Queen Elizabeth Granite|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: 1660-1655Ma.||||||07-NOV-08
30701|Queen Elizabeth Granite|63866|5|Briefly described|p59|Statherian|Statherian|Isan Orogeny, Sybella Batholith. A younger age of 1610 +/- 10 Ma (U-Pb TIMS, Page and Bell, 1986) was interpreted as a primary magmatic age for this unit; however, more recent SHRIMP work has shown it to be roughly 1660 Ma.|c. 1660 Ma (SHRIMP)|||||
30701|Queen Elizabeth Granite|67323|5|Briefly described|GIS attrib tbl, p12|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Sybella Domain, Mount Isa Inlier. Sybella Igneous Event.|1660 +/- 5 Ma.|Sybella Suite.|||Variably porphyritic medium to coarse biotite granite, leucocratic granite, gneiss.|
30701|Queen Elizabeth Granite|69591|5|Briefly described|p59|||Sybella Batholith.|1655 +/- 4 Ma (Connors and Page, 1995).||||Variably porphyritic medium to coarse biotite granite, leucocratic granite, gneiss.|
30701|Queen Elizabeth Granite|71592|5|Briefly described|Appendix A.|||Sybella Domain, Mount Isa Orogen.|1655+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30701|Queen Elizabeth Granite|72889|5|Briefly described|p1, p20, p23-25.|Statherian|Statherian|Younger than most Sybella Batholith granites. Magmatic ages from Connors and Page (1995).|1655+/-4 Ma, 1660+/-5 Ma|||||
83364|Queenslander Reef dyke|72983|5|Briefly described|p7, p52-55|Kungurian|Kungurian|[informal unit name]. Kennedy Igneous Association. Cape York region. Ebagoola Goldfield. Hosts Au quartz vein mineralisation.|277.7 +/- 3.6 Ma SHRIMP U-Pb|||Intrudes Lochs Gneiss.|Rhyolite; aphanitic, pervasively sericitised and cut by thin quartz veins.|
78314|Quilalar Supersequence|63866|5|Briefly described|p53, p56|Statherian|Statherian|Leichhardt Superbasin.|c. 1755-1740 Ma|||Equivalent to the McDermott Formation.||
78314|Quilalar Supersequence|65505|5|Briefly described|965, 980-1, Fig 8|Proterozoic|Proterozoic|Leichhardt River Fault Trough. Ballara Quartzite and Corella Formation are time-equivalent to Quilalar Formation. Transgressive systems tracts. Upper age: 1740 Ma.||||||
78314|Quilalar Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||Leichhardt Superbasin.|~1760-1740 Ma.|||Overlies Myally Supersequence. Is overlain by Big Supersequence.||
78314|Quilalar Supersequence|68021|5|Briefly described|p134 Fig 3, p135 Fig 4, p136|Statherian|Statherian|Leichhardt Superbasin. Fluviatile to shallow marine sediments. [Age by correlation with Corella Fm].|~1755 - ~1740 Ma|||Lateral equivalent to Ballera Quartzite, Corella Formation of the Eastern Succession.|Clean, well-sorted quartzite, well-bedded stromatolitic limestones, redeposited calcareous sandstones.|
78314|Quilalar Supersequence|68732|5|Briefly described|p159, p161, p166, p167, p171|Statherian|Statherian|Includes Quilalar Formation, Corella Formation, Ballara Quartzite, Mitakoodi Quartzite. Represents the oldest depositional package that can be correlated across the entire Mount Isa Inlier. Characterised by a transgressive and regressive cycle.|1748 +/- 4 Ma (maximum depositional age).|||||01-DEC-17
78314|Quilalar Supersequence|69591|5|Briefly described|p27, p32-34|||Leichhardt River Domain, Leichhardt Superbasin, Mount Isa Province. Includes Quilalar Formation, Ballara Quartzite and Corella Formation. Deposition followed the Myally Supersequence after a ~15 my hiatus.||||||
78314|Quilalar Supersequence|72912|5|Briefly described|p12.|||Of Leichhardt Superbasin. Followed the Myally Supersequence, deposition resumed after a 15 Ma hiatus (Neumann et al., 2005; Betts et al., 2006; Neumann and Fraser, 2007; Withnall and Hutton, 2013).|||Quilalar Formation,Corella Formation, Doherty Formation.||Shallow carbonate shelf sediments.|
24467|Quinine Spring Granite|23291|4|Described|p89 Fig. 3.8|||Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
24467|Quinine Spring Granite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 58. Assumed to be I-Type.||||||
24467|Quinine Spring Granite|23619|4|Described|p41 Table 2|Early Devonian|Silurian|Intrudes Einasleigh Metamorphics. Overlying unit McBride Basalt Group. Copperfield Batholith Province.||||||
24467|Quinine Spring Granite|39981|2|Defined|p104|Devonian|Silurian|Middle Proterozoic or Silurian-Devonian||||||
24467|Quinine Spring Granite|40542|6|Mentioned|p98|||||||||
24467|Quinine Spring Granite|41680|3|Fully described|p122|||||||||
24467|Quinine Spring Granite|43113|4|Described|Table 2 p26|Early Devonian|Silurian|||||||
24467|Quinine Spring Granite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
24467|Quinine Spring Granite|43259|4|Described|Appendix 1,p19.|Devonian|Silurian|age is Silurian -Early Devonian?||||||
24467|Quinine Spring Granite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
24467|Quinine Spring Granite|50202|5|Briefly described|Map legend|Late Silurian|Late Silurian|Biotite-muscovite granite and granodiorite.||||||
24467|Quinine Spring Granite|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Biotite-muscovite granite and granodiorite.||||||
24467|Quinine Spring Granite|68344|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Grey equigranular to porphyritic biotite-muscovite granite and granodiorite; local muscovite granite and pegmatite.|
24467|Quinine Spring Granite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian||||||Grey equigranular to porphyritic biotite-muscovite granite and granodiorite; local muscovite granite and pegmatite.|
24467|Quinine Spring Granite|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Grey equigranular to porphyritic biotite-muscovite granite and granodiorite; local muscovite granite and pegmatite.|
24467|Quinine Spring Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
23931|Quinton Formation|13996|5|Briefly described|p129, p132, p143, p145|Silurian|Silurian|Northern Tasman Fold Belt. Contains Llandovery-aged conodonts (species listed); tabulate corals. Hosts an undescribed Telychian-Sheinwoodian trilobite fauna, as well as the type species of Rhaxeros pollinctrix.|||||Includes isolated carbonates.|
23931|Quinton Formation|23032|4|Described|p22,23||Silurian|Equivalent to Poley Cow Formation.||||||
23931|Quinton Formation|23424|4|Described|Table 8.1 p334.||Llandovery|Age: Early Silurian (late Llandovery), to ?late Silurian; corals, conodonts, graptolites and trilobites. Laterally equivalent to the Poley Cow Formation. Of Graveyard Creek Group, Graveyard Creek Subprovince. Underlies Crooked Ck Conglomerate (c). 5000 m.||||||
23931|Quinton Formation|23430|5|Briefly described|p476|||Underlying Unit Crooked Creek Conglomerate. Broken River Province.||||||
23931|Quinton Formation|23431|5|Briefly described|p541|||||||||
23931|Quinton Formation|24029|5|Briefly described|p111, p113 Fig.1|Telychian|Telychian|Of Graveyard Creek Group. See also p115 Fig.3. Mapped seperately by these authors, but considered to be one and the same with Poley Cow Formation by others such as Simpson (1999) supported by Sloan et al (1995).||||||
23931|Quinton Formation|24577|4|Described|p751, p752 Fig. 1|Silurian|Silurian|Overlain by the Jack Formation. Overlies the Crooked Creek Conglomerate. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
23931|Quinton Formation|41260|3|Fully described|p40|||||||||
23931|Quinton Formation|41679|6|Mentioned|p253|||||||||
23931|Quinton Formation|41719|2|Defined|p217|Silurian||||||||
23931|Quinton Formation|41739|6|Mentioned|Fig.2|||||||||
23931|Quinton Formation|41740|6|Mentioned|p222|||||||||
23931|Quinton Formation|42031|5|Briefly described|p760|||||||||
23931|Quinton Formation|42054|6|Mentioned|p273|||||||||
23931|Quinton Formation|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
23931|Quinton Formation|42933|2|Defined|p56|Pridoli|Landovery|Of Graveyard Creek Group. Age Middle to Late Silurian.||||||14-APR-08
23931|Quinton Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Graveyard Creek Group.||||||
23931|Quinton Formation|50093|5|Briefly described|p329 Fig.2|Lochkovian|Early Silurian|||||||07-FEB-11
23931|Quinton Formation|63083|6|Mentioned|p218|Telychian|Telychian|Laterally equivalent to Poley Cow Formation in broken River region (Qld). Contains Llandovery trilobite fauna.||||||07-FEB-11
23931|Quinton Formation|63152|5|Briefly described|p120 Fig. 3|Silurian|Silurian|Arenite-dominated proximal turbiditic facies in the NW with conglomerate and allochthonous limestone blocks in lower part of sequence; shale and massive mudstone in NE; siltstone-arenite-conglomerate association in south.||||||10-APR-07
23931|Quinton Formation|67848|5|Briefly described|p14.|Early Silurian|Early Silurian|Broken River Province. Has late Llandovery fossils.||||Conformably overlies Crooked Creek Conglomerate.||
23931|Quinton Formation|68336|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Graveyard Creek Group.|Includes Magpie Creek Limestone Member.||Lithofeldspathic sandstone, polymictic conglomerate and mudstone; minor calcareous siltstone and sandstone and volcaniclastic siltstone and sandstone.|
23931|Quinton Formation|68341|5|Briefly described|Map legend.|Early Devonian|Silurian|Graveyard Creek Subprovince.||Unit in Graveyard Creek Group.|Includes Magpie Creek Limestone Member.||Lithofeldspathic sandstone, polymictic conglomerate and mudstone; minor calcareous siltstone and sandstone and volcaniclastic siltstone and sandstone.|
23931|Quinton Formation|69030|5|Briefly described|p6|Silurian|Silurian|Graveyard Creek Subprovince (Broken River Province).||Graveyard Creek Group||||
23931|Quinton Formation|69592|4|Described|p259-261, p263, p267|Telychian|Telychian|Northern Graveyard Creek Subprovince, Broken River Province. Fence diagram. Lithologies described in some detail, including a distinctive 100m thick interval of volcaniclastic sandstone, pebbly sandstone and conglomerate. >5km thick in the W, and over 2km in the E. Deep-marine fan deposits of turbidites and grain flows, with hemipelagic muds. Sedimentation rates up to 500m per million years indicate rapid subsidence. The upper part, including its Magpie Creek Member, was assigned by Mawson and Talent (2000) to their Ralph Flint Formation. Age from various fossil types.||||Conformably overlies Crooked Creek Conglomerate. Is overlain conformably by Shield Creek Formation. Laterally equivalent to Poley Cow Formation.|Medium- to very thick-bedded, coarse- to very coarse-grained sandstone with pebbly intervals in the upper part; mudstone or shale intervals, sometimes interlayered with thin- to medium-bedded sandstone up to 200m thick, also occur.|
41802|Racecourse Creek Gabbro|60481|5|Briefly described|Map Legend|Early Triassic|Late Permian - Correct|Dark grey to black, coarse to very coarse-grained hornblende gabbro.||||||
41802|Racecourse Creek Gabbro|61035|4|Described|p17 Tb. 2|Triassic|Permian|Intrudes Marlborough Metamorphics and Cleethorpes Granodiorite. Age: 241+/-5Ma (isotopic age). Consists of Dark grey to black, coarse to very coarse-grained hornblende gabbro.||||||07-FEB-11
41802|Racecourse Creek Gabbro|65388|4|Described|p430, p70 Fig. 28, p432|Early Triassic|Late Permian|Permian to Triassic? In contact with Cleethorpes Granodiorite. Relationship unknown. K-Ar hornblende age 245+/- 5 Ma (recalc from Webb & McDougall, 1968). Hornblende-augite gabbro.||||||
41802|Racecourse Creek Gabbro|68679|5|Briefly described|p308, p311, p424, p426|||Marlborough Province. A slightly arcuate, ~5km-long unit on the southern margin of Cleethorpes Granodiorite (relationship unknown).|245 +/- 5 Ma (K-Ar: Webb and McDougall, 1968).|||Intrudes Princhester Serpentinite.|Hornblende gabbro.|
30200|Racecourse Knob Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Parent: McBride Basalt Group. Age: >0.2Ma. Geological Province: Georgetown Region.||||||08-JUL-15
30200|Racecourse Knob Basalt|23619|4|Described|p28 table 1||Pleistocene|Olivine basalt. Large shield volcano. Of the McBride Basalt Group in the McBride Basalt Province.||||||
30200|Racecourse Knob Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
30200|Racecourse Knob Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
30200|Racecourse Knob Basalt|68576|5|Briefly described|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30200|Racecourse Knob Basalt|73115|6|Mentioned|p: 25, 27-29, 39, 43, 48, 53, 59, 65|Pleistocene|Pleistocene|McBride Basalt Province. Evidence for extensive pyroclastic behaviour.|0.2-0.21 Ma|||||
22723|Rackarock Rhyolite|23423|5|Briefly described|p305 Table 7.2||Early Permian|Wackara Volcanic Subgroup of Featherbed Volcanic Group.||||||
22723|Rackarock Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V100. A-Type.||||||
22723|Rackarock Rhyolite|23713|5|Briefly described|p20|||Of Wakara Volcanic Subgroup.||||||
22723|Rackarock Rhyolite|43083|5|Briefly described|p84|||Of the Wakara Volcanic Subgroup (Fetaherbed Volcanic Group).  Commonly contains clasts of andesite and basalt resembling units in the Nychum Volcanics.||||||17-JUN-09
22723|Rackarock Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
22723|Rackarock Rhyolite|43254|5|Briefly described|map legend||Early Permian|Of Wakara Volcanic Subgroup.||||||03-JUN-09
22723|Rackarock Rhyolite|43259|4|Described|Appendix 1,p10.||Early Permian|Of Wakara Volcanic Subgroup.||||||03-JUN-09
22723|Rackarock Rhyolite|43626|2|Defined|p90||Early Permian|Age about 278+/-3 Ma||||||
22723|Rackarock Rhyolite|60425|5|Briefly described|p44 Tb. 3|Early Permian|Early Permian|Informal unit of Wakara Volcanic Subgroup (Fatherbed Volcanic Group). Contains 3 informal subunits.||||||07-FEB-11
38877|Radley Nepheline Syenite|24489|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.||||||
38877|Radley Nepheline Syenite|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kggr].  Grey melanite-ferrohastingsite-aegirine nepheline syenite, lepidomelane-ferrohastingsite-sodalite nepheline syenite, lepidomelane-nepheline-ferrohastingsite-melanite sodalite syenite.||||||
38877|Radley Nepheline Syenite|68008|2|Defined|p399, p442, p444-449, p451, p457, p637|Early Cretaceous|Early Cretaceous|Defined in this study. Previously the Tollbar phase of the Ridley Syenite (Neale, 1968). Forms a triangular shaped mass c.1.5 km2 between Camp and Tollbar Creeks. Named after the Parish of Radley. The type area is to the SW, along a ridge leading up to Dawes Range. Forms low hills. Geophysics briefly described and modelled: contrasted with Monal Granodiorite. Geochemistry detailed: compared with Ridler Monzonite. Photomicrographs.||Glassford Igneous Complex.||Intrudes Ridler Monzonite and Littlemore Granodiorite. Correlated with Burns Spur Nepheline Monzosyenite.|A multi-phase intrusion, with three generations of dykes both coarser and finer than the host rock. K-feldspar is always dominant (40-75%); plagioclase is always greatly subordinate (<20%), with mafics from 5 to 30%.|
38877|Radley Nepheline Syenite|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Burns Spur Nepheline Monzosyenite, Judas Trachybasalt, Goondicum Gabbro, Ridler Monzonite, Tollbar Breccia, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
38877|Radley Nepheline Syenite|69594|5|Briefly described|p560-561|Cretaceous|Cretaceous|Whitsunday Volcanic Province.||Glassford Igneous Complex.||Intrudes Ridler Monzonite and Littlemore Granodiorite.|Multiphase intrusion of nepheline syenite variations (detailed); rocks are dominated by K-feldspar with or without subordinate plagioclase and varying proportions of nepheline and a sodalite group mineral.|
38877|Radley Nepheline Syenite|73450|4|Described|p11, p59-60, p62-66|early Cretaceous|early Cretaceous|Of Murray et al. (2012); studied in most detail by Neale (1968) wherein it was part of Ridler Syenite. Forms a small, triangular shaped outcrop area between Camp Creek and Tolbar Creek. Mineralogically and texturally heterogeneous. Composite unit with up to three generations of dykes both coarser and finer grained than the host rock. May be related to the Ridler Monzonite, Burns Spur Nepheline Monzosyenite, and Judas Trachybasalt.||Glassford Igneous Complex||Intrudes Ridler Monzonite and Littlemore Granodiorite.|Alkaline suite of granitoids containing hauyne and widespread nepheline.|
28949|Ramsay Crossing Member|39493|2|Defined|p98|late Eocene|middle Eocene|Mid to late Eocene||||||
28949|Ramsay Crossing Member|39997|6|Mentioned|p165|||||||||
28949|Ramsay Crossing Member|40116|6|Mentioned|p29|||||||||
28949|Ramsay Crossing Member|41273|6|Mentioned|p217|||||||||
28949|Ramsay Crossing Member|41927|5|Briefly described|p64|||||||||
28949|Ramsay Crossing Member|42021|6|Mentioned|p327|||||||||
28949|Ramsay Crossing Member|71092|5|Briefly described|p232-233|Eocene|Eocene|Contains fossil of Praecaryodes antiquata.||Rundle Formation.||||
28949|Ramsay Crossing Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
26118|Rangal Coal Measures|13516|6|Mentioned|p145 fig 3, p156|Late Permian|Late Permian|From Comet Ridge, Bowen Basin. Age: APP5006||||||14-NOV-12
26118|Rangal Coal Measures|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
26118|Rangal Coal Measures|22978|6|Mentioned|p148 Fig.1|||||||||
26118|Rangal Coal Measures|22979|5|Briefly described|p217|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22984|5|Briefly described|p275|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22985|5|Briefly described|p285|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22989|5|Briefly described|p310|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22990|5|Briefly described|p315 Table 1|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22992|6|Mentioned|p329|||||||||
26118|Rangal Coal Measures|22995|5|Briefly described|p361|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|22999|5|Briefly described|p389|Permian|Permian|||||||
26118|Rangal Coal Measures|23001|5|Briefly described|p409|||||||||
26118|Rangal Coal Measures|23002|6|Mentioned|p417|||||||||
26118|Rangal Coal Measures|23005|5|Briefly described|p439|Permian|Permian|||||||
26118|Rangal Coal Measures|23007|5|Briefly described|p454|Permian|Permian|||||||
26118|Rangal Coal Measures|23009|5|Briefly described|p463|||||||||
26118|Rangal Coal Measures|23012|6|Mentioned|p467|||||||||
26118|Rangal Coal Measures|23034|6|Mentioned|23|||||||||
26118|Rangal Coal Measures|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
26118|Rangal Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26118|Rangal Coal Measures|23161|4|Described|p32 table4||Late Permian|||||||
26118|Rangal Coal Measures|23430|5|Briefly described|p515-516|||Of Blackwater Group. Bowen Basin Province.||||||
26118|Rangal Coal Measures|23444|5|Briefly described|p190|||||||||
26118|Rangal Coal Measures|23769|4|Described|p862|Late Permian|Late Permian|Parent: Blackwater Group.  Geological Province: Bowen Basin.||||||
26118|Rangal Coal Measures|24093|4|Described|p177|Late Permian|Late Permian|Of the Blackwater Group.  Max. thickness: >200m.  Geological Province: Bowen Basin.||||||
26118|Rangal Coal Measures|29409|6|Mentioned|Table 1|||Equivalent in upper part of Bandanna Formation.||||||
26118|Rangal Coal Measures|29411|5|Briefly described|p201|||||||||
26118|Rangal Coal Measures|29412|5|Briefly described|p209|||Appears in a table, see also P210 and Fig.2.||||||
26118|Rangal Coal Measures|29727|6|Mentioned|p455|||||||||
26118|Rangal Coal Measures|30351|6|Mentioned|Fig.4|||Fig.4 on P32||||||
26118|Rangal Coal Measures|30508|6|Mentioned|p85|||Inferred reserves of non-coking coal||||||
26118|Rangal Coal Measures|30733|6|Mentioned|p372|||||||||
26118|Rangal Coal Measures|30851|6|Mentioned|p365|||||||||
26118|Rangal Coal Measures|30852|4|Described|Fig.2|||||||||
26118|Rangal Coal Measures|30915|6|Mentioned|p92|||||||||
26118|Rangal Coal Measures|30916|6|Mentioned|p92|||||||||
26118|Rangal Coal Measures|31079|6|Mentioned|p5|||||||||
26118|Rangal Coal Measures|31084|6|Mentioned|p12|||See also P21. U. Permian. Part Blackwater Gp.||||||
26118|Rangal Coal Measures|31167|6|Mentioned|Fig.2|||||||||
26118|Rangal Coal Measures|31261|6|Mentioned|p518|||||||||
26118|Rangal Coal Measures|31401|6|Mentioned|p30|||See also P32.||||||
26118|Rangal Coal Measures|31531|6|Mentioned|p13|||U.Permian. See also Table 1||||||
26118|Rangal Coal Measures|31620|5|Briefly described|p87|||See also P88-89||||||
26118|Rangal Coal Measures|31647|6|Mentioned|p356|||||||||
26118|Rangal Coal Measures|31649|6|Mentioned|p57|||||||||
26118|Rangal Coal Measures|31656|4|Described|Table 1|||U.Permian||||||
26118|Rangal Coal Measures|31690|4|Described|p42|||Mention P35.||||||
26118|Rangal Coal Measures|31979|6|Mentioned|p22|||||||||
26118|Rangal Coal Measures|32177|6|Mentioned|p146|||||||||
26118|Rangal Coal Measures|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26118|Rangal Coal Measures|32577|4|Described|p25|||U.Perm. See also P24,28,29.||||||
26118|Rangal Coal Measures|32689|6|Mentioned|Fig.2|||Strat. correlation table||||||
26118|Rangal Coal Measures|32730|6|Mentioned|p48|||||||||
26118|Rangal Coal Measures|32834|6|Mentioned|Table 3|||||||||
26118|Rangal Coal Measures|33250|5|Briefly described|p139|||||||||
26118|Rangal Coal Measures|33251|4|Described|p10|||See also P2||||||
26118|Rangal Coal Measures|33390|4|Described|p6|||||||||
26118|Rangal Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
26118|Rangal Coal Measures|34276|6|Mentioned|p42|||Perm. See also P51||||||
26118|Rangal Coal Measures|35138|6|Mentioned|p8|||||||||
26118|Rangal Coal Measures|35141|6|Mentioned|Fig.1|||||||||
26118|Rangal Coal Measures|35266|6|Mentioned|p192|||||||||
26118|Rangal Coal Measures|35433|4|Described|p28|||||||||
26118|Rangal Coal Measures|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin. Lithology described P186.||||||
26118|Rangal Coal Measures|35810|6|Mentioned|p545|||||||||
26118|Rangal Coal Measures|35822|6|Mentioned|Fig.3|||||||||
26118|Rangal Coal Measures|35873|6|Mentioned|Fig.9|||See also P119.||||||
26118|Rangal Coal Measures|35922|6|Mentioned|p46|||||||||
26118|Rangal Coal Measures|35937|6|Mentioned|p619|||||||||
26118|Rangal Coal Measures|36172|6|Mentioned|Appendix|||||||||
26118|Rangal Coal Measures|36254|6|Mentioned|p34|||||||||
26118|Rangal Coal Measures|37065|6|Mentioned|p32|||||||||
26118|Rangal Coal Measures|37069|6|Mentioned|p66|||||||||
26118|Rangal Coal Measures|37070|4|Described|p74|||||||||
26118|Rangal Coal Measures|37072|4|Described|p92|||||||||
26118|Rangal Coal Measures|37073|6|Mentioned|p99|||||||||
26118|Rangal Coal Measures|37074|6|Mentioned|p105|||||||||
26118|Rangal Coal Measures|37075|6|Mentioned|p110|||||||||
26118|Rangal Coal Measures|37076|4|Described|p120|||||||||
26118|Rangal Coal Measures|37077|5|Briefly described|p131|||See also P130.||||||
26118|Rangal Coal Measures|37078|6|Mentioned|p134|||||||||
26118|Rangal Coal Measures|37080|5|Briefly described|p150|||||||||
26118|Rangal Coal Measures|37612|3|Fully described|p290|||See also Fig.3.||||||
26118|Rangal Coal Measures|37726|6|Mentioned|Fig.2|||||||||
26118|Rangal Coal Measures|37749|6|Mentioned|p186|||||||||
26118|Rangal Coal Measures|38518|6|Mentioned|Fig.3|||||||||
26118|Rangal Coal Measures|38657|6|Mentioned|p128|||||||||
26118|Rangal Coal Measures|38737|6|Mentioned|p156|||||||||
26118|Rangal Coal Measures|38948|4|Described|p453|||||||||
26118|Rangal Coal Measures|38958|5|Briefly described|p493|||||||||
26118|Rangal Coal Measures|38971|4|Described|p543|||||||||
26118|Rangal Coal Measures|39212|4|Described|p14|||Correlated with Baralaba CM in part P14. See also P12||||||
26118|Rangal Coal Measures|39252|6|Mentioned|p26|||See also P28||||||
26118|Rangal Coal Measures|39257|5|Briefly described|p57|||||||||
26118|Rangal Coal Measures|39258|5|Briefly described|p73|||||||||
26118|Rangal Coal Measures|39261|6|Mentioned|Fig.6|||||||||
26118|Rangal Coal Measures|39266|6|Mentioned|p222|||||||||
26118|Rangal Coal Measures|39267|6|Mentioned|p240|||||||||
26118|Rangal Coal Measures|39269|6|Mentioned|Fig.1|||||||||
26118|Rangal Coal Measures|39270|4|Described|p281|||||||||
26118|Rangal Coal Measures|39273|6|Mentioned|Fig. 2|||||||||
26118|Rangal Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9||||||
26118|Rangal Coal Measures|39491|6|Mentioned|p24|||||||||
26118|Rangal Coal Measures|40087|6|Mentioned|p234|||||||||
26118|Rangal Coal Measures|40146|6|Mentioned|p181|||||||||
26118|Rangal Coal Measures|40251|6|Mentioned|Fig.2|||||||||
26118|Rangal Coal Measures|40321|6|Mentioned|p17|||||||||
26118|Rangal Coal Measures|40539|6|Mentioned|p164|||||||||
26118|Rangal Coal Measures|41191|5|Briefly described|p284|||||||||
26118|Rangal Coal Measures|41226|6|Mentioned|Table 1|||||||||
26118|Rangal Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
26118|Rangal Coal Measures|41689|6|Mentioned|Table 1|||||||||
26118|Rangal Coal Measures|41921|6|Mentioned|Fig.1|||||||||
26118|Rangal Coal Measures|42187|6|Mentioned|p319|||||||||
26118|Rangal Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
26118|Rangal Coal Measures|42251|5|Briefly described|p39|||||||||
26118|Rangal Coal Measures|42252|5|Briefly described|p50|||||||||
26118|Rangal Coal Measures|42255|6|Mentioned|p233|||||||||
26118|Rangal Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
26118|Rangal Coal Measures|42257|5|Briefly described|Table 1 P263|||||||||
26118|Rangal Coal Measures|42259|6|Mentioned|p16|||||||||
26118|Rangal Coal Measures|42584|6|Mentioned|p75|||||||||
26118|Rangal Coal Measures|42641|6|Mentioned|p109|||||||||
26118|Rangal Coal Measures|42648|6|Mentioned|p40|||||||||
26118|Rangal Coal Measures|42662|5|Briefly described|p85|||||||||
26118|Rangal Coal Measures|42701|3|Fully described|p71|||||||||
26118|Rangal Coal Measures|42932|4|Described|p3|||||||||
26118|Rangal Coal Measures|43000|5|Briefly described|p113|||||||||
26118|Rangal Coal Measures|43994|14|Not recorded|Map Legend||Late Permian|Part of the Blackwater Group.||||||
26118|Rangal Coal Measures|44245|5|Briefly described|Map Legend||Permian|||||||
26118|Rangal Coal Measures|44337|5|Briefly described|Map Legend||Late Permian|Lithology.||||||
26118|Rangal Coal Measures|44618|14|Not recorded|p511||Permian|Unit of Blackwater Group. Ref. to Malone et al. 1965 and Olgers et al. 1965.||||||
26118|Rangal Coal Measures|44629|14|Not recorded|p560|||Blackwater. Fused coal. No age given.||||||
26118|Rangal Coal Measures|44630|14|Not recorded|p492,494,497|||Part of Blackwater Group.||||||
26118|Rangal Coal Measures|44631|14|Not recorded|p205||Late Permian|||||||
26118|Rangal Coal Measures|44721|14|Not recorded|p28-36||Late Permian|||||||
26118|Rangal Coal Measures|45071|3|Fully described|Table 12|||||||||
26118|Rangal Coal Measures|45095|3|Fully described|p11|||||||||
26118|Rangal Coal Measures|48898|2|Defined|p54|Late Permian|Late Permian|See also PP2,44,51 etc||||||
26118|Rangal Coal Measures|48947|4|Described|p8|||||||||
26118|Rangal Coal Measures|49644|5|Briefly described|Table|||||||||
26118|Rangal Coal Measures|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin and north Comet Ridge.||||||04-FEB-08
26118|Rangal Coal Measures|60472|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Of the Blackwater Group. Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.||||||16-SEP-04
26118|Rangal Coal Measures|60659|5|Briefly described|p21|Late Permian|Late Permian|Of the Blackwater Group. Sandstone, coal, siltstone, carbonaceous shale, mudstone and pebbly sandstone; with plant fossils throughout. Conformably overlie Fort Cooper C.M. Geological Province: Bowen Basin.||||||07-FEB-11
26118|Rangal Coal Measures|61232|5|Briefly described|p119,  Tb.1, p126 |Late Permian|Late Permian|Overlies German Creek and/or Moranbah Coal Measures||||||
26118|Rangal Coal Measures|61612|6|Mentioned|p274, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
26118|Rangal Coal Measures|62921|6|Mentioned|p883|||Bowen Basin. Mis-spelt as Rangol. ||||Overlies Burngrove Formation.||
26118|Rangal Coal Measures|63713|6|Mentioned|p1523|||||||Equivalent to Bandana Formation.||
26118|Rangal Coal Measures|64099|5|Briefly described|p373, p374 Fig 5|Permian|Permian|Underlies Sagittarius Sandstone. Geol Prov: Bowen Basin.||||||
26118|Rangal Coal Measures|64665|5|Briefly described|p53 Fig.2.|Late Permian|Late Permian|Bowen Basin.||||Overlies Fort Cooper Coal Measures. Is overlain by Rewan Group.||
26118|Rangal Coal Measures|65003|6|Mentioned|p6|||||||Equivalent to the Baralaba Coal Measures.||30-MAR-12
26118|Rangal Coal Measures|65388|4|Described|p201-202, 200|Late Permian|Late Permian|Uppermost Blackwater Group, Bowen Basin. Throughout basin, except SE where rocks assigned to Baralaba Coal Measures instead. Mapped as the Elphinstone Coal Measures by Reid (1946). Overlie the Fort Cooper Coal Measures. Gradational contact with overlying Rewan Group. Malone & others (1969) gave a type section in Deep Creek 5km west of Taurus homestead S of Blackwater. 100-300m thick. Sandstone, coal, siltstone, carbonaceous mudstone, mudstone (locally cherty), and rare pebbly sandstone. Age: Tatarian with palynomorphs assigned to APP5.||||||
26118|Rangal Coal Measures|67402|6|Mentioned|p21, p45, p80 tbl BWN1|Wuchiapingian|Wuchiapingian|Bowen Basin. See also p85, p85 tbl BWN2, p272.||Blackwater Group||Overlain by the Rewan Group. Overlies the Fort Cooper Coal Measures, the Burngrove Formation, Fair Hill Formation and the Mac Millan Formation.||
26118|Rangal Coal Measures|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Rewan Formation. Underlain by Fort Copper Coal Measures.||
26118|Rangal Coal Measures|67788|6|Mentioned|p23, 30|Permian|Permian|Photograph of large alluvial channel deposits; southward basin-axial paleoflow.||||||
26118|Rangal Coal Measures|68139|6|Mentioned|p32|Permian|Permian|Bowen Basin. Group 5 coals. Hosts coal seam gas-producing fields.||||||
26118|Rangal Coal Measures|68202|6|Mentioned|p176|Permian|Permian|Bowen Basin.||Blackwater Group.||||
26118|Rangal Coal Measures|68679|5|Briefly described|p353, p377, p381, p383-384|Early Triassic|Early Triassic|Jensen (1975). Connors-Auburn Province. Covers most of the northern Bowen Basin. 240m thick. Alluvial plain sediments. Red clasts indicate sediments were sourced from the Rewan Group. Properties of the coal are described in some detail.||Blackwater Group.||Overlies Fort Cooper Coal Measures and Burngrove Formation. Is overlain by Rewan Group.|Feldspatholithic sandstone, interbedded siltstone/sandstone, carbonaceous siltstone and mudstone, coal.|
26118|Rangal Coal Measures|69760|5|Briefly described|p139|Permian|Permian|Bowen Basin. Marks the end of the Permian.|||Elphinstone, Hynds seams.|Is overlain by the Rewan Group.|Interbedded sandstone, siltstone, mudstone, tuff, coal.|
26118|Rangal Coal Measures|70330|5|Briefly described|p10-13, 16-18|Late Permian|Late Permian|Bowen Basin. Appears in the text as RCM after the first couple of mentions. Thickens towards the south (due to increased seam splitting and clastic inter-seam sediments).||Blackwater Group.|Vermont Upper seam; Leichhardt seam; Phillips seam.|||
26118|Rangal Coal Measures|70815|6|Mentioned|p3-4, 6-7, 11|||Bowen Basin. Vitrinite reflectance values mapped.||||||
26118|Rangal Coal Measures|70861|5|Briefly described|p36-37,40,44-45|Late Permian|Late Permian|Of Bowen Basin.||Unit of Blackwater Group.||Underlain by Fort Cooper Coal Measures/Burngrove Formation. Correlable to Bandana Formation.|Coal seams with  sandstone, fine grained heterolithics and intrusions.|
26118|Rangal Coal Measures|70940|5|Briefly described|p843-844, p846, p850|Permian|Permian|Bowen Basin.||Blackwater Group.||Overlies Yarrabee Tuff.||
26118|Rangal Coal Measures|71265|5|Briefly described|p589|Induan|Induan|Bowen Basin.||||Overlies Fort Cooper Coal Measures. Is overlain by Rewan Group.||
26118|Rangal Coal Measures|71276|6|Mentioned|p295-296|||||||Overlies Yarrabee Tuff.||
26118|Rangal Coal Measures|71282|6|Mentioned|p459|Permian|Permian|||||||
26118|Rangal Coal Measures|71701|5|Briefly described|p155|||Northern Area, Bowen Basin.||||Unconformably overlain by the Rewan Group. Overlies the Fort Cooper Coal Measures.||
26118|Rangal Coal Measures|72297|5|Briefly described|p694 Fig.10.8, p695-696, p703, p705,p750|Permian|Permian|Bowen Basin. Indicative properties of export coking, thermal and PCI coals tabulated. Potential for future CSG production.|||Aries, Castor, Pollux, Orion, Pisces, Roper, Middlemount, Tralee, Leichhardt, Vermont Seams; Elphinstone, Hynds and Wolfgang seams.|Overlies Fort Cooper Coal Measures and Burngrove Formation. Is overlain by Rewan Group.||
26118|Rangal Coal Measures|73036|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.|
26118|Rangal Coal Measures|73037|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.|
26118|Rangal Coal Measures|73038|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.|
26118|Rangal Coal Measures|73040|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Calcareous sandstone, calcareous shale, mudstone, coal, concretionary limestone.|
26118|Rangal Coal Measures|73163|6|Mentioned|p468|||Bowen Basin.||||Overlies the Yarrabee Tuff.||02-FEB-22
26118|Rangal Coal Measures|73246|6|Mentioned|p190-192, p194, p199|Upper Permian|Upper Permian|Bowen Basin, northeast and northwest.||Blackwater Group|Yarrabee Tuff|Underlain by Fort Cooper Coal Measures and Burngrove Formation. Overlain by Rewan Group.||
26118|Rangal Coal Measures|73304|6|Mentioned|p71, p73, p77|||Bowen Basin. [Top?] boundary marks a major extinction of peat-producing plants.||||||
26118|Rangal Coal Measures|73305|6|Mentioned|p547, p548 Fig.1, p550, p560-561|Late Permian|Late Permian|Bowen Basin. Abbreviated to RCM in text. Boundary with the underlying Fort Cooper Coal Measures defined by the Yarrabee Tuff. Includes the Upper Vermont Seam.||||Overlies the Fort Cooper Coal Measures.|Includes low ash content coal.|
26118|Rangal Coal Measures|73625|5|Briefly described|p3, p5 Fig.3, p13, 20-22, p25|Permian|Permian|See also p23 Fig.14E. Taroom Trough, Bowen Basin. The middle part of this unit records a regressive-transgressive cycle.||||Overlies Fort Cooper Coal Measures or Burngrove Formation. Is overlain by the 'Marker Mudstone'/Rewan Group. Equivalent to Bandanna Formation.|Includes localised, plant-fossil-rich, permineralised peats associated with silica-rich ash deposits.|
80924|Range Creek Granite|69592|6|Mentioned|p283|||||Mount Webster Supersuite.||||
32036|Raspberry Creek Formation|22482|4|Described|p487, p490||Middle Devonian|of Capella Creek Group||||||
32036|Raspberry Creek Formation|23522|5|Briefly described|p250 Fig 6|Givetian|Eifelian|||||||
32036|Raspberry Creek Formation|24491|4|Described|p16|||Of Capella Creek Group. Overlies Mount Warner Volcanics. Overlain unconformably by Mount Hoopbound, Balaclava and Mount Alma Formations.||||||
32036|Raspberry Creek Formation|24615|5|Briefly described|CD|Middle Devonian|Middle Devonian|[Dcr].  Predominantly basaltic to andesitic (rarely dacitic and rhyolitic) volcaniclastic sandstone and conglomerate, minor silicified siltstone and fossiliferous limestone; rare andesite lava.||||||
32036|Raspberry Creek Formation|50197|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32036|Raspberry Creek Formation|50208|5|Briefly described|Map Legend|Devonian|Devonian|Includes: Ginger Creek Member.  Of the Capella Creek Group.||||||
32036|Raspberry Creek Formation|50209|5|Briefly described|Map Legend|Devonian|Devonian|||||||
32036|Raspberry Creek Formation|50317|5|Briefly described|Map Legend|Devonian|Devonian|Of the Capella Creek Group.  Predominantly basaltic to andesitic (rarely dacitic and rhyolitic) volcaniclastic sandstone and conglomerate.||||||09-JUN-04
32036|Raspberry Creek Formation|60557|5|Briefly described|p19 Fig. 5b|Middle Devonian|Late Silurian|Of the Capella Creek Group.||||||09-JUN-05
32036|Raspberry Creek Formation|61147|5|Briefly described|p377, p379, pp381-383.|Middle Givetian|Latest Eifelian|Widely exposed unit. Middle varcus subzone.||Unit in Capella Creek Group.||Intruded by Mount Morgan trondhjemite and Bouldercombe Complex.|A thick pile of andesitic lavas, sedimentary rocks with minor but locally prominent limestone.|
32036|Raspberry Creek Formation|61730|5|Briefly described|p1001|||Youngest unit in Capella Creek Group. Comprises volcaniclastic sandstone and conglomerate sourced from basalt and andesite, with a more felsic component at the top; this latter where it is more extensive forms the Ginger Creek Member.||||||
32036|Raspberry Creek Formation|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Mount Morgan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
32036|Raspberry Creek Formation|65388|6|Mentioned|p67, 72|Middle Devonian|Middle Devonian|Includes basalts of broadly similar chemistry to Campwyn Volcanics, Tanderra Volcanics.||||||
32036|Raspberry Creek Formation|68008|2|Defined|p16, p26-27, p32, p34-40, p61, p89, p366|Middle Devonian|Middle Devonian|See also p381, p395-396, p476, p628, p648-650. Yarrol Project Team (1997). Named after Raspberry Creek, SE of Mount Morgan. Type section, on the property "Belgamba", is from GR243800 7387500 to GR244400 7387500 on the Mount Morgan 100k sheet; 464m thick. Measured type section diagram. Maximum thickness 1350m. Previously the Capella Creek beds (Messenger and Taube, 1994 after Kirkegaard et al., 1970). Forms a belt 75 x 14km of hilly country with steep-sided deep creeks. Geochemistry discussed and contrasted with that of Craigilee beds. Shallow-marine (oceanic island arc) setting. Diverse coral species listed. Micropaleontology table. Structural data discussed. Is intruded by Mount Morgan Trondhjemite, Kabra Quartz Monzodiorite, Bajool and Cecilwood Quartz Diorites, and units of Galloway Plains Igneous Complex.||Capella Creek Group.|Ginger Creek Member.|Conformably overlies Mount Warner Volcanics. Is overlain unconformably by Mount Hoopbound, Balaclava, Mount Alma Formations. See Comments.|Sandstone, conglomerate and breccia, mostly volcaniclastic and with andesitic and basaltic sources; local basalt lava and minor siltstone and fossiliferous limestone; rare accretionary lapilli tuff.|
32036|Raspberry Creek Formation|68679|4|Described|p315-316, p401, p403 Tb.5.8, p425-426|Givetian|Givetian|Murray et al. (2012), for the upper part of the Capella Creek beds. Forms a belt 75km long and up to 14km wide, SE from near Kabra to Ayrdrie homestead. Contains a rich and diverse Givetian fossil fauna, particularly corals and conodonts. Ocean island-arc setting.||Capella Creek Group.|Ginger Creek Member.|Is overlain unconformably by Mount Hoopbound Formation. Is intruded by Rocky Point Granodiorite, Bajool Quartz Diorite and Cecilwood Quartz Diorite, and Kabra Quartz Monzodiorite.|Sandstone, granule to pebble conglomerate and breccia, local basalt lava, minor siltstone and limestone, and rare accretionary lapilli tuff. Volcaniclastic rocks of basaltic and andesitic derivation predominate.|
32036|Raspberry Creek Formation|73143|6|Mentioned|p17|Givetian|Givetian|Contains rugose coral Nardophyllum immanum (Blake, 2010).||||||
36230|Rattler Granite|23291|5|Briefly described|p101 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Froghollow Suite. Intrudes Rudd Granite, Gingerella Volcanics. Geological Province: Georgetown Region.||||||01-JUL-15
36230|Rattler Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36230|Rattler Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 379. I-Type.||||||
36230|Rattler Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36230|Rattler Granite|23624|4|Described|p10|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Rudd Granite.||||||17-DEC-13
36230|Rattler Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, porphyritic biotite monzogranite; mafic enclaves common.|
36230|Rattler Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, porphyritic biotite monzogranite; mafic enclaves common.|
36508|Rattlesnake Island granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 154.||||||
41104|Ravenscraig Gabbro|50301|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
41104|Ravenscraig Gabbro|65388|2|Defined|p330-331, p256, 273, p301 Fig 98|Early Triassic|Late Permian|Interpreted to intrude Glen View Quartz Monzodiorite, Rockdale Granite. Interpreted to post-date Mungunal Granite. Age uncertain, but considered a relatively young intrusion. Mainly fine to coarse-grained, porphyritic hornblende gabbro. ||||||
41104|Ravenscraig Gabbro|68679|5|Briefly described|p407, p419|||A ~4 km2 pluton cropping out west of the main Rawbelle Batholith among Carboniferous-Permian plutons.||||Intrudes Glen View Quartz Monzodiorite and Rockdale Granite.|Porphyritic hornblende gabbro; well-developed igneous layering.|
69347|Ravenshoe Suite|60425|5|Briefly described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of O'Briens Creek Supersuite. Contains Neds Gully and Ravenshoe Granites. I-type.||||||07-FEB-11
26119|Ravenswood Granodiorite Complex|22611|6|Mentioned|P186||Early Ordovician|||||||
26119|Ravenswood Granodiorite Complex|22630|6|Mentioned|p12|||||||||
26119|Ravenswood Granodiorite Complex|22675|5|Briefly described|p91|||Loworth-Ravenswood Block||||||
26119|Ravenswood Granodiorite Complex|22844|6|Mentioned|p12,50|||After Paine 1971, now covered under current Fat Hen Creek and Gorge Creek Complexes.||||||
26119|Ravenswood Granodiorite Complex|22847|5|Briefly described|p 6|||||||||
26119|Ravenswood Granodiorite Complex|24613|6|Mentioned|p90|Devonian|Ordovician|Unconformably overlain by Collopy Formation.||||||07-FEB-11
26119|Ravenswood Granodiorite Complex|30148|6|Mentioned|p7|||||||||
26119|Ravenswood Granodiorite Complex|30149|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian or Lower Devonian age||||||
26119|Ravenswood Granodiorite Complex|30151|4|Described|Table 1|||See also Fig.3.  454+-30 m.y.||||||
26119|Ravenswood Granodiorite Complex|30914|6|Mentioned|Map legend|Devonian|Silurian|Ordovician - Devonian||||||
26119|Ravenswood Granodiorite Complex|31659|6|Mentioned|p102|||Mid-Ordovician||||||
26119|Ravenswood Granodiorite Complex|31813|5|Briefly described|p5|||See also p16. Ordovician - Lower Devonian.||||||23-APR-08
26119|Ravenswood Granodiorite Complex|31984|6|Mentioned|Map legend|Early Devonian|Middle Ordovician|Middle Ord.-L.Dev.||||||
26119|Ravenswood Granodiorite Complex|31999|6|Mentioned|p126|||Table 11||||||
26119|Ravenswood Granodiorite Complex|32169|6|Mentioned|Table 2|||||||||
26119|Ravenswood Granodiorite Complex|32359|5|Briefly described|p733|||||||||
26119|Ravenswood Granodiorite Complex|32360|6|Mentioned|p742|||||||||
26119|Ravenswood Granodiorite Complex|32493|6|Mentioned|Map legend|Early Devonian|Middle Ordovician|M.Ord.-L.Dev.||||||
26119|Ravenswood Granodiorite Complex|32556|4|Described|Table 2|||||||||
26119|Ravenswood Granodiorite Complex|33202|6|Mentioned|p22|||||||||
26119|Ravenswood Granodiorite Complex|33644|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
26119|Ravenswood Granodiorite Complex|33648|5|Briefly described|p10|||M.Ord?||||||
26119|Ravenswood Granodiorite Complex|34409|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician, Upper Silurian, Lower Devonian||||||
26119|Ravenswood Granodiorite Complex|34894|6|Mentioned|p477|||||||||
26119|Ravenswood Granodiorite Complex|34975|6|Mentioned|p909|||||||||
26119|Ravenswood Granodiorite Complex|35154|6|Mentioned|Fig.3|||||||||
26119|Ravenswood Granodiorite Complex|35304|6|Mentioned|p605|||||||||
26119|Ravenswood Granodiorite Complex|35322|6|Mentioned|p416|||||||||
26119|Ravenswood Granodiorite Complex|36154|6|Mentioned|Fig.3|||||||||
26119|Ravenswood Granodiorite Complex|36472|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26119|Ravenswood Granodiorite Complex|36561|6|Mentioned|p542|||||||||
26119|Ravenswood Granodiorite Complex|37144|6|Mentioned|p14|||||||||
26119|Ravenswood Granodiorite Complex|37451|6|Mentioned|Table 2|||See also P380||||||
26119|Ravenswood Granodiorite Complex|37570|6|Mentioned|p123|||||||||
26119|Ravenswood Granodiorite Complex|37573|6|Mentioned|p201|||See also Fig.5||||||
26119|Ravenswood Granodiorite Complex|37764|6|Mentioned|Table 1|||||||||
26119|Ravenswood Granodiorite Complex|39129|6|Mentioned|p181|||||||||
26119|Ravenswood Granodiorite Complex|39445|5|Briefly described|p66|||Gold production. See aslo p62 & Table 12.||||||23-APR-08
26119|Ravenswood Granodiorite Complex|39686|4|Described|p75|||See also Fig.1||||||
26119|Ravenswood Granodiorite Complex|39731|5|Briefly described|p29|||||||||
26119|Ravenswood Granodiorite Complex|39732|6|Mentioned|p29|||||||||
26119|Ravenswood Granodiorite Complex|39734|4|Described|p21|||||||||
26119|Ravenswood Granodiorite Complex|39735|6|Mentioned|p16|||||||||
26119|Ravenswood Granodiorite Complex|39986|6|Mentioned|p73|||||||||
26119|Ravenswood Granodiorite Complex|39995|6|Mentioned|p217|||||||||
26119|Ravenswood Granodiorite Complex|40623|5|Briefly described|p91|||||||||
26119|Ravenswood Granodiorite Complex|40746|5|Briefly described|p343|||||||||
26119|Ravenswood Granodiorite Complex|40787|5|Briefly described|p322|||||||||
26119|Ravenswood Granodiorite Complex|40920|6|Mentioned|p71|||||||||
26119|Ravenswood Granodiorite Complex|40958|6|Mentioned|p160|||||||||
26119|Ravenswood Granodiorite Complex|40974|6|Mentioned|p205|||||||||
26119|Ravenswood Granodiorite Complex|41246|6|Mentioned|Map legend|Devonian|Ordovician|||||||
26119|Ravenswood Granodiorite Complex|41272|5|Briefly described|M 1of1 A08|||||||||
26119|Ravenswood Granodiorite Complex|41774|6|Mentioned|p30|||||||||
26119|Ravenswood Granodiorite Complex|41805|6|Mentioned|Fig.2|||||||||
26119|Ravenswood Granodiorite Complex|41825|6|Mentioned|p206|||||||||
26119|Ravenswood Granodiorite Complex|42031|5|Briefly described|p764|||||||||
26119|Ravenswood Granodiorite Complex|42245|6|Mentioned|p30|||||||||
26119|Ravenswood Granodiorite Complex|42689|5|Briefly described|map legend|Early Paleozoic||||||||07-NOV-08
26119|Ravenswood Granodiorite Complex|42750|5|Briefly described|p32|||Same as Ravenswood Granodiorite?||||||23-APR-08
26119|Ravenswood Granodiorite Complex|43093|5|Briefly described|Appendix 1|||Previous nomenclature for many intrusive units.||||||23-APR-08
26119|Ravenswood Granodiorite Complex|43095|5|Briefly described|Plate 1|||||||||
26119|Ravenswood Granodiorite Complex|43103|6|Mentioned|p17|||||||||
26119|Ravenswood Granodiorite Complex|43121|5|Briefly described|Fig.1.|||||||||
26119|Ravenswood Granodiorite Complex|43391|5|Briefly described|Map legend|Devonian|Ordovician|Geological Province: Lolworth-Ravenswood Block.  Biotite granite and and biotite-hornblende to hornblende-biotite granodiorite to tonalite.||||||23-JUN-04
26119|Ravenswood Granodiorite Complex|43589|6|Mentioned|p25|||Intruded by Pall Mall Granite.||||||23-APR-08
26119|Ravenswood Granodiorite Complex|43706|5|Briefly described|p18|||||||||
26119|Ravenswood Granodiorite Complex|43763|6|Mentioned|p749|||||||||
26119|Ravenswood Granodiorite Complex|45073|4|Described|p15|||Gold (p65).||||||23-APR-08
26119|Ravenswood Granodiorite Complex|45086|6|Mentioned|p57|||See also P58. Ordovician.||||||
26119|Ravenswood Granodiorite Complex|45151|6|Mentioned|p4|||||||||
26119|Ravenswood Granodiorite Complex|48903|3|Fully described|p17|||M.Ord. ? Rb/Sr age. See also Table 1.||||||
26119|Ravenswood Granodiorite Complex|48904|2|Defined|p13|Early Devonian|Silurian|Ordovician - Early Devonian||||||
26119|Ravenswood Granodiorite Complex|48914|3|Fully described|p20|||||||||
26119|Ravenswood Granodiorite Complex|48922|3|Fully described|p17|||age||||||
26119|Ravenswood Granodiorite Complex|60659|5|Briefly described|p9|Middle Ordovician|Late Cambrian|Mainly granodiorite, with subordinate granite, adamellite, diorite and gabbro. Intrusives of the Macrossan Province.||||||07-FEB-11
26119|Ravenswood Granodiorite Complex|62521|5|Briefly described|p2|||Previously Ravenswood Granodiorite. Has also been named Ravenswood Batholith by Hutton et al (1990). Geological Province: Ravenswood Batholith. Age: 470+/-30Ma and 408+/-30Ma.||||||14-JAN-08
26119|Ravenswood Granodiorite Complex|65706|4|Described|p9 Fig.3; p10; Tb.1 p13,16,17|Early Devonian|Late Cambrian|See also p23, p42 Fig.10, p53, p55, p123, p127, p150. Paine et al., 1974. Hosts Cu mineralisation and several styles of gold mineralisation.||||Intrudes Cape River Metamorphics, Mount Windsor Volcanics (Seventy Mile Range Group).|Granite, microgranite, granodiorite, tonalite, foliated in places, with minor quartz diorite, diorite, trondhjemite, gabbro, pegmatite and aplite.|
26865|Rawbelle batholith|36333|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic||||||
26866|Raymond Sandstone|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
26866|Raymond Sandstone|34389|4|Described|Table 1|||Lower Carboniferous||||||
26866|Raymond Sandstone|34390|4|Described|Table 1|||Lower Carboniferous||||||
26866|Raymond Sandstone|34392|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26866|Raymond Sandstone|40623|5|Briefly described|p110|||||||||
26866|Raymond Sandstone|43029|5|Briefly described|p24|||||||||
26866|Raymond Sandstone|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||underlies Star of Hope Formation; overlies Mount Hall Formation||23-DEC-11
26866|Raymond Sandstone|43213|6|Mentioned|p77, p238|||Veevers et al., (1964). Originally named the Flaggy Sandstone Group by Shell (Queensland) Development Pty Ltd (1952) then Raymond Flaggy Sandstone (Hill, 1957); subsequently Raymond Formation (Olgers, 1972). Rocks tentatively assigned to this unit disconformably overlie Silver Hills Volcanics. Geophysics described.||||||
26866|Raymond Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
26866|Raymond Sandstone|43990|14|Not recorded|Map Legend||Early Carboniferous|||||||
26866|Raymond Sandstone|43994|14|Not recorded|Map Legend|||||||||
26866|Raymond Sandstone|43998|4|Described|p20|Carboniferous|Devonian|||||||
26866|Raymond Sandstone|44081|14|Not recorded|p43|||||||||
26866|Raymond Sandstone|44091|14|Not recorded|p39,46,Tb.3||Early Carboniferous|||||||
26866|Raymond Sandstone|44331|14|Not recorded|Map Legend||Early Carboniferous|||||||
26866|Raymond Sandstone|44337|5|Briefly described|Map Legend||Early Carboniferous|Lithology.||||||
26866|Raymond Sandstone|45071|3|Fully described|Table 1|||Name changed to Raymond Formation (Olgers,1972)||||||
26866|Raymond Sandstone|45073|6|Mentioned|p36|||Refers Veerers et al. (1964b) Now Raymond Fm.||||||
26866|Raymond Sandstone|48843|14|Not recorded|p.14|||Formation of Drummond Beds, missing from Clermont area.||||||
26866|Raymond Sandstone|48845|2|Defined|p7,10-1,13,16,18-20,|||p23-27,Fig.10,map. Overlies Mount Hall Conglomerate; underlies Ducabrook Formation. = 'Flaggy Sandstone Group' = 'Raymond Flaggy Sandstone'.||||||
26866|Raymond Sandstone|48900|3|Fully described|p16|||||||||
26866|Raymond Sandstone|48908|6|Mentioned|p21||Early Carboniferous|||||||
26866|Raymond Sandstone|48915|6|Mentioned|Table 1|||Devonian - Carboniferous||||||
26866|Raymond Sandstone|62074|6|Mentioned|p3|||||||||
26866|Raymond Sandstone|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Flaggy quartzose sandstone, siltstone and minor limestone.||||||
26866|Raymond Sandstone|68326|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Mount Hall Formation. Is overlain conformably by Star of Hope Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|02-DEC-13
26866|Raymond Sandstone|68328|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Is intruded by Withersfield Granite. Is overlain conformably by Star of Hope Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|
26866|Raymond Sandstone|68411|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||Shown as lateral equivalent of the Mount Hall Formation. Conformably overlain by the Star of Hope Formation. Conformably underlain by the Silver Hills Volcanics.|Flaggy quartzose sandstone, siltstone, and minor limestone.|
26866|Raymond Sandstone|68412|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Mount Hall Formation. Is conformably overlain by Star of Hope Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|23-JUN-15
26866|Raymond Sandstone|68413|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||Conformably underlain by the Mount Hall Formation. Conformably overlain by the Star of Hope Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|
26866|Raymond Sandstone|68423|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|Drummond Basin. This unit is incorrectly colour-coded in the "Palaeozoic Units" inset on the sheet.||||Conformably overlies Mount Hall Formation. Is overlain conformably by Star of Hope Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|
26866|Raymond Sandstone|68482|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlain by the Star of Hope Formation. Conformably underlain by the Mount Hall Formation.|Flaggy quartzose sandstone, siltstone and minor limestone.|
26866|Raymond Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Mount Hall, Scartwater and Telemon Formations, are all mapped under the symbol, Cd2.||||||
26866|Raymond Sandstone|68900|6|Mentioned|p38-p40, p65|||Obsolete name, see Raymond Formation.||||||
26866|Raymond Sandstone|69379|5|Briefly described|map legend|Early Carboniferous|Late Devonian||||||Flaggy quartzose sandstone, siltstone and minor limestone|
36103|Reamba Volcanics|23291|4|Described|p38, p93 Tb. 3.11|||Probably Early Permian. Geological Province: Georgetown Region.||||||08-JUL-15
36103|Reamba Volcanics|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province. Age: Early Permian?||||||
36103|Reamba Volcanics|23510|5|Briefly described|Map Legend||Early Permian|||||||
36103|Reamba Volcanics|23616|5|Briefly described|Table 3 p57||Late Carboniferous|Age: Late Carboniferous? Unconformable on Proterozoic granite; overlain by Tertiary Bulimba Formation. Dargalong Province.||||||30-AUG-04
36103|Reamba Volcanics|24485|4|Described|p40, p42 Tb.7|Early Permian|Early Permian|Overlying Unit: Bulimba Formation (unconformable). Underlying Unit: Fig Tree Hill Granite Complex. Max Thickness: >200m? Geological Province: Hodgkinson Province||||||
36103|Reamba Volcanics|24486|5|Briefly described|Map legend|Early Permian|Early Permian|||||||
36103|Reamba Volcanics|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Georgetown Inlier.||||||
36103|Reamba Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
36103|Reamba Volcanics|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.||||||
36103|Reamba Volcanics|69593|6|Mentioned|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
73022|Red Bull Formation|63152|5|Briefly described|p120 Fig. 3|||Of the Jack Group (Graveyard Creek Supergroup). Overlies Dark Dog Limestone; overlain by Coral Gardens Formation. Red arenites.||||||10-APR-07
75159|Red Dome microgranite|60425|4|Described|p280-1 Appdx. |||Part of Ootann Supersuite? Age: 322+/-3Ma (SHRIMP, Perkins and Kennedy, 1998). I-type. V.fine-gr., porphyritic rhyolite to microgranite, +fine-gr., sparsely porphyritic aplitic microgranite with scattered quartz+feldspar phenocrysts - more lith.detail||||||07-FEB-11
75757|Red Hill Creek Granodiorite|70740|5|Briefly described|p127, p128|||Outcrop characteristics and distribution briefly discussed. |||||Medium-grained, moderately porphyritic hornblende-biotite granodiorite with minor sphene, allanite and scattered mafic inclusions.|
75757|Red Hill Creek Granodiorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Pale pinkish grey, medium-grained, moderately porphyritic hornblende-biotite granodiorite; with minor sphene, traces of allanite?, and scattered mafic inclusions to 50 cm.|
80925|Red Knob Granite|69592|6|Mentioned|p283|||||Mount Webster Supersuite.||||
36278|Red River Rhyolite|23291|4|Described|p93 Fig. 3.9|Early Permian|Late Carboniferous|See also Red River rhyolite. Parent: Bulleringa Volcanic Subgroup. Age: 289+/-2Ma. Geological Province: Georgetown Region.||||||08-JUL-15
36278|Red River Rhyolite|23510|5|Briefly described|Map Legend||Early Permian|of Bulleringa Volcanic Subgroup, Scardons Volcanic Group.||||||
38786|Redbank Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
22738|Redcap Dacite|23291|5|Briefly described|p37|||Of the Featherbed Volcanic Group. Geological Province: Georgetown Region.||||||08-JUL-15
22738|Redcap Dacite|23423|4|Described|p307 Table 7.3||Late Carboniferous|Of the Featherbed Volcanic Group. Intruded by Ruddygore and Belgravia Granodiorites.||||||01-JUN-09
22738|Redcap Dacite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group, Kennedy Province.||||||01-JUN-09
22738|Redcap Dacite|23616|5|Briefly described|Table 3 p51||Late Carboniferous|Faulted against and apparently unconformable on Hodgkinson Fm rocks; intruded by Ruddygore and Belgravia Granodiorites. Of Featherbed Volcanic Gp, Hodgkinson Fm. Thick. ~3600 m.||||||01-JUN-09
22738|Redcap Dacite|24485|5|Briefly described|p43 Tb.7|Late Carboniferous|Late Carboniferous|Parent: Featherbed Volcanic Group. Max Thickness: ~3600m||||||
22738|Redcap Dacite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group.  Geological Province: Kennedy Province.||||||
22738|Redcap Dacite|24487|5|Briefly described|Map legend|||||||||
22738|Redcap Dacite|43087|6|Mentioned|p83|||||||||
22738|Redcap Dacite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ignimbrites of the Featherbed Volcanic Group.||||||15-JUN-06
22738|Redcap Dacite|43259|4|Described|Appendix 1,p12.||Late Carboniferous|Of Featherbed Volcanic Group.||||||29-APR-09
22738|Redcap Dacite|43567|6|Mentioned|Fig.2,p398||Late Carboniferous|||||||
22738|Redcap Dacite|43626|2|Defined|p10,41||Late Carboniferous|||||||
22738|Redcap Dacite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22738|Redcap Dacite|60425|4|Described|p48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Gp. Comprises 4 informal subunits. Faulted against and apparently unconformable on Hodgkinson Fm. Intruded by Ruddygore + Belgravia Granodiorites. Welded, mod'ly crystal-poor to very crystal-rich, rhyolitic to andesitic ignimbrite||||||07-FEB-11
22739|Reddicliffe Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
22739|Reddicliffe Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
22739|Reddicliffe Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 326. I-Type.||||||
22739|Reddicliffe Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
22739|Reddicliffe Granite|23624|4|Described|p18|Permian|Carboniferous|Parent: Ootann Supersuite.||||||30-MAR-15
22739|Reddicliffe Granite|43087|6|Mentioned|p40|||||||||
22739|Reddicliffe Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22739|Reddicliffe Granite|43259|4|Described|Appendix 1,p39.||Carboniferous|Late? Carboniferous in age.||||||
22739|Reddicliffe Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. 3 subunits:(1) mainly even-gr., rarely porph'ic biotite granite; (2) even-gr.-slightly porph'ic biotite leucogranite, + (3) even-gr.to slightly porph'ic biotite leucogranite+mafic enclaves - more lith. detail||||||30-MAR-15
22739|Reddicliffe Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. An un-named geophysical subdivision of this unit is mapped separately and described as a probable variant of this unit's lithology.||Unit in Ootann Supersuite.|||Pink to cream, medium- to coarse-grained biotite granite; rare microgranite.|
22739|Reddicliffe Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. An un-named geophysical subdivision of this unit is mapped separately and described as a probable variant of this unit's lithology.||Unit in Ootann Supersuite.|||Pink to cream, medium- to coarse-grained biotite granite; rare microgranite.|
22739|Reddicliffe Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Five variants are mapped separately.||Unit in Ootann Supersuite.|||Pink to cream or pale brown, mostly fine- to medium-grained, mainly even-grained biotite leucogranites to monzogranite; rare microgranite.|
22743|Redlands Granite|23049|3|Fully described|p27|Early Devonian|Late Silurian|of Amarrra Suite.||||||
22743|Redlands Granite|23283|2|Defined|p22|Devonian|Silurian|||||||
22743|Redlands Granite|23422|5|Briefly described|p216 Table 6.10|Early Devonian|Late Silurian|Of Amarra Supersuite.||||||
22743|Redlands Granite|23505|5|Briefly described|Map legend|Devonian|Silurian|of Amarra Supersuite.||||||
22743|Redlands Granite|69592|5|Briefly described|p293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~8 km2; best exposed on Mount Oweenee.||Amarra Suite.|||Pink to cream, muscovite leucogranite; comprises quartz, large poikilitic K-feldspar, lath-shaped plagioclase, muscovite and minor garnet.|
39574|Redshirt Granite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Littlemore Suite.  Geological Province: Yarrol Province.||||||
39574|Redshirt Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgae].  Pink medium- to coarse-grained hornblende-biotite granite with minor tourmaline pegmatite.||||||
39574|Redshirt Granite|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
39574|Redshirt Granite|68008|2|Defined|p331, p372, p378-379, p381-382, p384-385|Early Triassic|Permian|See also p387-389, p484, p528, p629. New unit, named after Mount Redshirt which is composed entirely of the intrusion. An oblong intrusion, 4.5 x 2.5 km, 40km NNE of Biloela. The type area appears to be the entire exposure, where boulders and tors are present. Resistant unit; forms prominent peak (Mount Redshirt). Differentiated from surrounding Dumgree Tonalite by its distinctive, extremely strong radiometric response (and topography); geophysics modelled. Geochemistry compared with Mount Seaview Igneous Complex and Miriam Vale Granodiorite. Probably the source of mineralisation at the Fig Tree Provisional Goldfield.|251 +/- 4 Ma (U-Pb zircon; Fanning, 2012).|Galloway Plains Igneous Complex.||Intrudes Rocky Point Granodiorite, Dumgree Tonalite.|Pink, medium- to coarse-grained, hornblende-biotite monzogranite with patches of tourmaline-bearing pegmatite. Rhyolite dyke swarms. Post-tectonic.|
39574|Redshirt Granite|68679|5|Briefly described|p424-425|Early Triassic|Permian|Yarrol Province. Forms an oblong, ~4.5 x 2.5 km pluton. Hosts small gold deposits.|251 +/- 4 Ma (SHRIMP U-Pb zircon: Fanning, 2012).|Galloway Plains Igneous Complex.||Intrudes Dumgree Tonalite.|Hornblende-biotite granite.|
39574|Redshirt Granite|71592|5|Briefly described|Appendix A.||||251+/-4 Ma (SHRIMP U-Pb zircon).||||Granite.|
82638|Reedy Gabbro|71628|5|Briefly described|p19: 150-151|||New name, after Reedy Creek, a local watercourse. Located 19 km WSW of Ballandean. Comprises three dominant bodies in a series cropping out over ~6 km. Very limited geochemistry (one analysis) briefly described. Hosts two Sn deposits, not genetically linked to the Reedy Gabbro.||Reedy Suite.||Intrudes Texas beds.|Medium-grained gabbro; extensively altered.|
22746|Reedybed Granite|23049|3|Fully described|p24|Early Devonian|Late Silurian|Of the Amarra Suite.||||||14-APR-08
22746|Reedybed Granite|23283|2|Defined|p21|Devonian|Silurian|||||||
22746|Reedybed Granite|23422|5|Briefly described|p216 Table 6.10|Early Devonian|Late Silurian|Of Amarra Supersuite.||||||
22746|Reedybed Granite|23505|5|Briefly described|Map legend|Devonian|Silurian|Of Amarra Supersuite.||||||14-APR-08
22746|Reedybed Granite|69592|5|Briefly described|p293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~90-100 km2.||Amarra Suite.|||Medium-grained biotite and muscovite-biotite granite.|
36635|Reid River granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 499.  I-Type.||||||
36159|Reids Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36159|Reids Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
36159|Reids Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Included in Emuford Granite on most recent maps. Pale pink, fine-grained, porphyritic biotite granite.  I-type.||||||07-FEB-11
79313|Repeater Station Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Williams Igneous Event.||Williams Supersuite.|||Strongly albitised granite.|
79313|Repeater Station Granite|69591|6|Mentioned|p60|||Mount Isa Province.|||||Strongly albitised granite.|
79313|Repeater Station Granite|70353|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Strongly albitised granite.|
79313|Repeater Station Granite|70354|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Strongly albitised granite.|
22751|Retchford Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Supersuite.||||||01-JUN-09
22751|Retchford Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Of the Ootann Supersuite.||||||01-JUN-09
22751|Retchford Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 441. I-Type.||||||
22751|Retchford Granite|23616|6|Mentioned|Table 6 p72|||Of Ootann Supersuite.||||||
22751|Retchford Granite|43060|5|Briefly described|Table 6|||Of Ootann Supersuite.||||||01-JUN-09
22751|Retchford Granite|43083|5|Briefly described|p255|||Of the Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
22751|Retchford Granite|43087|2|Defined|p65|Late Carboniferous||Of Ootann Supersuite||||||24-NOV-08
22751|Retchford Granite|43151|5|Briefly described|Map legend||Late Carboniferous|Of the Ootann Suite (Ootann Supersuite).||||||15-JUN-06
22751|Retchford Granite|43259|4|Described|Appendix 1,p47.||Late Carboniferous|||||||
22751|Retchford Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).I-type. Pale pink to pinkish grey, fine- to med.-gr., even-gr.to slightly porphyritic (hornblende-) biotite granite; slightly altered in places; several small Au mines present.||||||07-FEB-11
22751|Retchford Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to pinkish grey, fine- to medium-grained, even-grained to slightly porphyritic (hornblende-)biotite monzogranite; slightly altered in places.|
22752|Retire Monzodiorite|23423|5|Briefly described|p239|||||||||
22752|Retire Monzodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~301-302 Ma, Rb-Sr.  Of the Almaden Supersuite.||||||01-JUN-09
22752|Retire Monzodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 352. I-Type.||||||
22752|Retire Monzodiorite|23616|5|Briefly described|Table 3 p48, p67|||Of Almaden Supersuite.||||||
22752|Retire Monzodiorite|43060|6|Mentioned|p92|||||||||
22752|Retire Monzodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Retire Suite (Almaden Supersuite). Predominantly quartz monzodiorite.  Age: 301Ma.||||||15-JUN-06
22752|Retire Monzodiorite|43259|4|Described|Appendix 1,p41.||Carboniferous|Age is 301 Ma.||||||
22752|Retire Monzodiorite|60425|4|Described|p49 Tb.3, p282-3 Appdx. |Late Carboniferous|Late Carboniferous|Of Retire Suite (Almaden Supersuite). Intruded Boonmoo Volcanic Subgroup. Age: ~301-302Ma (Rb-Sr). Fine- to medium-grained, slightly porphyritic quartz monzodiorite, with various combinations of hypersthene, augite, biotite and hornblende. I-type.||||||07-FEB-11
22752|Retire Monzodiorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A reversely magnetised part of this unit is mapped separately. ||Unit in Almaden Supersuite.|||Dark grey, fine- to medium-grained, slightly porphyritic quartz monzodiorite to quartz diorite?; with various combinations of hypersthene, augite, hornblende and biotite.|
22752|Retire Monzodiorite|68576|6|Mentioned|Q_11: p11|||Forms low-lying country. Similar age to Boonmoo Volcanic Subgroup (i.e. c.308 Ma).||||||
22752|Retire Monzodiorite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|305 Ma.|Almaden Supersuite.||||
30427|Retire Suite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Supersuite (Almaden Supersuite).||||||15-JUN-06
30427|Retire Suite|60425|5|Briefly described|p76, p282-3 Appdx.|Early Permian|Late Carboniferous|Of the Almaden Supersuite. Contains Retire Monzodiorite, Muldiva Quartz Monzodiorite, Prices Dam Igneous Complex and Mount Wandoo Granodiorite. Dominated by mafic rocks - diorites and monzodiorites, but also contains some felsics. I-type.||||||07-FEB-11
77636|Retreat Supersuite|43213|6|Mentioned|p95, p116-121, p124|||In the Retreat Batholith.|||Includes Kilmarnock, Karmoo and Mount Newsome Suites.|||
77636|Retreat Supersuite|68553|6|Mentioned|Map legend|Late Devonian|Middle Devonian|||||||
77636|Retreat Supersuite|68900|6|Mentioned|p4|Late Devonian|Middle Devonian|Drummond Basin.||||||
24471|Revenue Granite|22734|4|Described|p291-8||Statherian|Cause of mid-crustal hydrothermal system aureole during emplacement.||||||13-OCT-08
24471|Revenue Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|1735+/-2Ma.||||||13-OCT-08
24471|Revenue Granite|24197|5|Briefly described|p32, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24471|Revenue Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24471|Revenue Granite|37862|4|Described|p586|||||||||
24471|Revenue Granite|38350|4|Described|p17|||||||||
24471|Revenue Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24471|Revenue Granite|38658|6|Mentioned|p153|||||||||
24471|Revenue Granite|39445|6|Mentioned|Table 2|||||||||
24471|Revenue Granite|40840|6|Mentioned|Map legend|||||||||
24471|Revenue Granite|42879|6|Mentioned|p214|||||||||
24471|Revenue Granite|45161|5|Briefly described|p31|||||||||
24471|Revenue Granite|45166|5|Briefly described|p34|||||||||
24471|Revenue Granite|49009|2|Defined|p37|Proterozoic|Proterozoic|Previously mapped as Wonga Granite (Carter & Opik,1963).||||||
24471|Revenue Granite|49041|5|Briefly described|Table 2|||||||||
24471|Revenue Granite|50100|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Burstall Suite (Wonga Batholith). Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||13-OCT-08
24471|Revenue Granite|50536|5|Briefly described|p1.4, 5.3, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||07-NOV-08
24471|Revenue Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Hornblende-biotite granite.||||||
24471|Revenue Granite|65505|6|Mentioned|980|Proterozoic|Proterozoic|Age: 1735 +/-2 Ma (U-Pb zircon).||||||
24471|Revenue Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot.. Mary Kathleen Domain, Mount Isa Inlier. Wonga/Burstall Igneous Event.|1735 +/- 2 Ma.|Wonga Suite, Burstall Suite.|||Medium to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite|
24471|Revenue Granite|67497|5|Briefly described|p889, p900 Tb.7, p909, p911 Fig.20|Statherian|Statherian|Age from sample FBMI-5605.|1722 +/- 5 Ma U/Pb SHRIMP zircon.|Of the Burstall Suite.|||A-type granite spatially associated with minor Au-Cu mineralisation and possibly the product of relatively fractionated, late-stage melts of the Burstall magmatic event.|07-MAY-12
24471|Revenue Granite|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1735 +/- 2 Ma.|||||
24471|Revenue Granite|69591|5|Briefly described|p60||||1735 +/- 2 Ma (Curtin Uni. Tech., unpub. data)|Burstall Suite.|||Medium- to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite.|
24471|Revenue Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1735+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
24471|Revenue Granite|72596|6|Mentioned|p1-2, p23-24, p40, p46|Statherian|Statherian|Correlated with / compositionally similar to the granitic component of the Mount Erle Complex and Myubee Igneous Complex, and the Overlander and Burstall granites (see Bultitude et al., 1982; Blake et al., 1984).|1735 +/- 2 Ma|Burstall Suite||Cross-cuts the Corella Formation||
24471|Revenue Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Medium to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite.Coarse-grained to graphic quartz-feld spar pegmatite; minor calc-silcates.|
24471|Revenue Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Medium to coarse-grained leucocratic granite; minor aplite, pegmatite, microgranite.Coarse-grained to graphic quartz-feld spar pegmatite; minor calc-silcates.|
24471|Revenue Granite|72799|6|Mentioned|p1, p5, p10, p19, p24|Statherian|Statherian|Bierlein et al. (2011) reported slightly younger SHRIMP zircon emplacement ages (1718-1722 Ma) for parts of the unit suggesting it might be composite. Passchier (1992) suggested this unit is slightly older than the nearby Myubee Igneous Complex, based on structural criteria.|ca. 1735-1740 Ma|||Coeval[?] with Myubee Igneous Complex.||
24471|Revenue Granite|73413|6|Mentioned|App.1|Statherian|Statherian|U-Pb SHRIMP age of 1735 +/- 2 Ma reported by Geoscience Australia.|1735 +/- 2 Ma|||||
24471|Revenue Granite|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Mary Kathleen Domain.|1735+/-2 Ma, 1722+/-5 Ma||||Felsic intrusive.|
24471|Revenue Granite|73529|5|Briefly described|p2 Fig.1, p4-5, p7, p9-11, p13-14|Statherian|Statherian|Elongate N-S trending body, 13 km long and 3-3.5 km wide. Used to constrain age of the proposed Wonga Orogeny, timing of emplacement interpreted as prior to or early during D1 based on deformation. See also Revenue granite.|1741+/-6 Ma Pb/Pb zircon|Burstall Suite||Intrudes Corella Formation|Intrusive unit.|
24471|Revenue Granite|73553|4|Described|p2, p8, p14, p39, p42-44, p59,|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Previously mapped as Burstall Granite. Small, folded pluton interpreted as a sill-like body ~1 km thick. Contains alteration zones of albitised or scapolitised granite. May be a composite unit based on ages. Mostly mottled white and pale blue tones on radiometric images. Very low responses on aeromagnetic images. Additional age of 1722+/-6 Ma (SHRIMP). See also p39, p42, p64, p71, p110, p135, p146-p154, p157-159, p164-165, p168, p173, p176, p221, p266.|1717+/-11 Ma LAICPMS, 1735+/-2 Ma U-Pb SHRIMP|Burstall Suite||Intrudes Corella Formation|Pinkish to pale grey, fine to medium grained, even grained to slightly porphyritic, deformed and extensively recrystallised. Well-developed foliation. Aplite intrusion on SW margin.|03-FEB-23
36220|Rices Creek Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Saucebottle Suite. Intrudes Saucebottle, Gelaro, Junevale Granites; intruded(?) by McCord Granite (O'Brien's Creek Supersuite). Geological Province: Georgetown Region.||||||08-JUL-15
36220|Rices Creek Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36220|Rices Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 347. I-Type.||||||
36220|Rices Creek Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36220|Rices Creek Granite|23624|5|Briefly described|p17|Permian|Carboniferous|Parent: Ootann Supersuite.||||||01-JUL-15
36220|Rices Creek Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey or pink to red (altered), medium-grained, even-grained to slightly porphyritic biotite granite.|
36220|Rices Creek Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey or pink to red (altered), medium-grained, even-grained to slightly porphyritic biotite granite.|
36220|Rices Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Grey or pink to red (altered), medium-grained, even-grained to slightly porphyritic biotite granite.|
38865|Ridler Monzonite|24488|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.||||||
38865|Ridler Monzonite|24489|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.||||||
38865|Ridler Monzonite|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kggi].  Pale grey leococratic biotite-augite-h'blende syenite, biotite-h'blende-augite monzonite, ferrohastingsite-aegirine monzanite, biotite-h'blende-augite quartz monzonite, h'blende quartz monzodiorite, h'blende-biotite-augite gabbro and monzogabbro.||||||
38865|Ridler Monzonite|68008|2|Defined|p399-400, p403, p439-445, p447, p451|Early Cretaceous|Early Cretaceous|See also p454, p456-457, p460, p637. Originally the Ridler Syenite of Neale (1968), for a complex syenitic intrusion in the headwaters of Ridler Creek. More recent mapping has subdivided these rocks into 7 units. This unit is 7 x 2.5 km along the N side of Ridler Creek, after which it is named. The type area is Mount Sugarloaf and the lower ridges immediately to the W. Forms hilly, locally steep dissected country. Geophysics described in some detail and modelled: contrasted with Monal Granodiorite. Geochemistry detailed; compared/contrasted with some other units of the Igneous Complex. Photomicrographs. Hosts copper anomalies.|141 +/- 4 Ma (biotite: Green and Webb, 1974).|Glassford Igneous Complex.||Intrudes Rockhampton Group, Monal and Littlemore Granodiorites. Is intruded by every other unit of Glassford Igneous Complex.|Covers the full compositional range from syenite, through monzonite and quartz monzodiorite, to monzogabbro and gasbbro. Each lithology described in detail.|
38865|Ridler Monzonite|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Burns Spur Nepheline Monzosyenite, Judas Trachybasalt, Radley Nepheline Syenite, Goondicum Gabbro, Tollbar Breccia, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
38865|Ridler Monzonite|68679|5|Briefly described|p432|||Bundaberg-Agnes Water-Biloela region.||||Adjacent to Monal Granodiorite.||
38865|Ridler Monzonite|69594|4|Described|p560-561|Cretaceous|Cretaceous|Whitsunday Volcanic Province.|141 +/- 4 Ma (K-Ar biotite: Green and Webb, 1974).|Glassford Igneous Complex.||Intrudes Rockhampton Group, Monal and Littlemore Granodiorites. Is intruded by Burns Spur Nepheline Monzosyenite and Radley Nepheline Syenite.|Alkali-rich and locally feldspathic. Compositionally diverse. Mostly monzonite but also syenite, through monzonite and quartz monzodiorite, to monzogabbro and gabbro (detailed).|
38865|Ridler Monzonite|73422|6|Mentioned|p10|Berriasian|Berriasian|A K-Ar biotite age of 141 Ma K-Ar was previously reported by Bryan and Purdy (2013).|141 Ma K-Ar biotite|||||
38865|Ridler Monzonite|73450|4|Described|p59-66|Valanginian|Berriasian|Of Murray et al. (2012). Equates to the Mount Sugarloaf phase of the superseded Ridler syenite of Neale (1968). Forms a NE-trending pluton NNE of Monto; forms hilly, locally steep country dissected by Ridler Creek and its tributaries. Average composition is monzonite syenite, which is found mainly on Mount Sugarloaf. Distinguished from Triassic granitoids in the complex by lower abundances of quartz and mafic minerals, finer grainsize, and the lack of alteration. Intruded by all the other Cretaceous units of the Glassford Igneous Complex. Yielded a K-Ar biotite age of 141 +/- 4 Ma (Green and Webb, 1974). Surrounds Judas Trachybasalt. May be related to the Radley Nepheline Syenite, Burns Spur Nepheline Monzosyenite, and Judas Trachybasalt.|141 +/- 4 Ma K-Ar|Glassford Igneous Complex||Intrudes Rockhampton Group, Monal Granodiorite, and Littlemore Granodiorite. Intruded by Radley Nepheline Syenite and Burns Spur Nepheline Monzosyenite.|Includes a compositional range from syenite, through monzonite and quartz monzodiorite, to monzogabbro and gabbro.|
23940|Ringwood Park Microgranite|23032|6|Mentioned|p14|||||||||
23940|Ringwood Park Microgranite|23074|5|Briefly described|p738 (Fig 2), p740|||||||||
23940|Ringwood Park Microgranite|23291|4|Described|p89 Fig. 3.8|Ordovician|Ordovician|Intrudes Balcooma Metavolcanics and Lugano Metavolcanics. Intruded by Dido Tonalite (Dido Supersuite - Silurian). Geological Province: Georgetown Region.||||||08-JUL-15
23940|Ringwood Park Microgranite|23430|5|Briefly described|p469|||||||||
23940|Ringwood Park Microgranite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 69. I-Type.||||||
23940|Ringwood Park Microgranite|23619|4|Described|p42 Table 2|Ordovician|Late Cambrian|Intrudes Balcooma Metavolcanics. Intruded by Dido Tonalite. Also see p7. Overlying unit Bally Knob Volcanics and McBride Basalt Group - unconformable. Georgetown Province.||||||
23940|Ringwood Park Microgranite|41675|2|Defined|p53|Middle Ordovician||||||||
23940|Ringwood Park Microgranite|42054|6|Mentioned|p272|||||||||
23940|Ringwood Park Microgranite|42216|5|Briefly described|Fig.1 P425|||||||||
23940|Ringwood Park Microgranite|42279|4|Described|p21|||See also Fig.3||||||
23940|Ringwood Park Microgranite|42933|6|Mentioned|p220|||||||||
23940|Ringwood Park Microgranite|43113|4|Described|Table 2 p27|||U-Pb zircon dating-(Withnall & others).Late Cambrian or Middle Ordivician||||||
23940|Ringwood Park Microgranite|43253|5|Briefly described|map legend|Ordovician|Cambrian|||||||
23940|Ringwood Park Microgranite|43259|4|Described|Appendix 1,p20.||Ordovician|Middle Ordovician?||||||
23940|Ringwood Park Microgranite|43772|6|Mentioned|p786|Ordovician|Cambrian|||||||
23940|Ringwood Park Microgranite|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Porphyritic microgranite.||||||
23940|Ringwood Park Microgranite|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province.|||||Pink, foliated, equigranular to porphyritic microgranites and biotite granites.|
23940|Ringwood Park Microgranite|68731|5|Briefly described|p151 Fig 3.51, p152, p154|Ordovician|Ordovician|Refers to several small plutons at the northern end of the Balcooma Metavolcanic Group that formed as high-level intrusions and were comagmatic with the volcanic succession.||||Intrudes the Balcooma Metavolcanic Group. Intruded by the Dido Tonalite.|Comprises biotite microgranite, grading into fine-grained granite.|17-JUL-14
26871|Ripley Road Sandstone|12597|5|Briefly described|p491, p492 Tb.1, p496|Pliensbachian|Hettangian|Clarence-Moreton Basin. Up to 1200m thick.||Unit in Woogaroo Subgroup.|||Massive, cross-bedded, fine- to coarse-grained, sub-labile to quartzose sandstone.|
26871|Ripley Road Sandstone|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
26871|Ripley Road Sandstone|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rhaetian|Of the Woogaroo Subgroup (Bundamba Group). Quartz arenite, granule conglomerate. Max. thickness: 150m. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|22865|6|Mentioned|Fig.22.10ap318|||||||||
26871|Ripley Road Sandstone|23435|5|Briefly described|p66|||of Woogaroo Subgroup.||||||
26871|Ripley Road Sandstone|23799|5|Briefly described|p46|Late Triassic|Late Triassic|See also p48 Fig. 3.  Of the Woogaroo Subgroup.  Overlies Raceview Formation.  Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|23811|5|Briefly described|Map Legend|Pliensbachian|Hettangian|Of Woogaroo Subgroup.  Thick-bedded, fine- to medium- to very coarse-grained quartz-rich sandstone and quartz-rich granule conglomerate.  A grey clay matrix is characteristic of fresh rock.  Geological Province: Clarence-Moreton Basin.||||||09-MAY-13
26871|Ripley Road Sandstone|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Late Triassic|Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 400m.||||||
26871|Ripley Road Sandstone|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
26871|Ripley Road Sandstone|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|29385|6|Mentioned|p82|||Jurassic.||||||
26871|Ripley Road Sandstone|30086|5|Briefly described|p4|||Triassic age. Part of Bundamba Group.||||||
26871|Ripley Road Sandstone|30302|6|Mentioned|p415|||Refers to Staines(1964)||||||
26871|Ripley Road Sandstone|30458|6|Mentioned|p2|||||||||
26871|Ripley Road Sandstone|30463|6|Mentioned|p466|||See also P471||||||
26871|Ripley Road Sandstone|30464|6|Mentioned|p3|||||||||
26871|Ripley Road Sandstone|30465|6|Mentioned|p4|||||||||
26871|Ripley Road Sandstone|30466|6|Mentioned|p14|||Triassic age||||||
26871|Ripley Road Sandstone|30470|6|Mentioned|p459|||||||||
26871|Ripley Road Sandstone|30472|6|Mentioned|p132|||Pollen distribution||||||
26871|Ripley Road Sandstone|30474|6|Mentioned|p251|||Correlation chart||||||
26871|Ripley Road Sandstone|30475|6|Mentioned|Fig.14.3|||||||||
26871|Ripley Road Sandstone|30477|6|Mentioned|p461|||||||||
26871|Ripley Road Sandstone|30915|6|Mentioned|p100|||||||||
26871|Ripley Road Sandstone|31118|4|Described|p320|||||||||
26871|Ripley Road Sandstone|31259|6|Mentioned|p325|||Refers Staines (1964)||||||
26871|Ripley Road Sandstone|32136|6|Mentioned|p5|||Miospores||||||
26871|Ripley Road Sandstone|32176|6|Mentioned|p2|||Bundamba Gp. See also P3, Figs. 2&3.||||||
26871|Ripley Road Sandstone|32179|6|Mentioned|p3|||Trias.||||||
26871|Ripley Road Sandstone|32180|6|Mentioned|Table 1|||||||||
26871|Ripley Road Sandstone|32492|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
26871|Ripley Road Sandstone|33381|6|Mentioned|p118|||See also P122||||||
26871|Ripley Road Sandstone|33476|6|Mentioned|p99|||||||||
26871|Ripley Road Sandstone|34010|6|Mentioned|Cor. chart|||U.Triassic||||||
26871|Ripley Road Sandstone|34354|6|Mentioned|p3|||Triassic. See also P12.||||||
26871|Ripley Road Sandstone|34505|6|Mentioned|p3|||Bundamba Group. See Figs.8,9,10,11||||||
26871|Ripley Road Sandstone|35101|6|Mentioned|p51|||||||||
26871|Ripley Road Sandstone|35866|6|Mentioned|p399|||||||||
26871|Ripley Road Sandstone|36243|6|Mentioned|Table 8A|||||||||
26871|Ripley Road Sandstone|36779|6|Mentioned|p7|||||||||
26871|Ripley Road Sandstone|36825|6|Mentioned|p12|||||||||
26871|Ripley Road Sandstone|37111|6|Mentioned|Table 1|||||||||
26871|Ripley Road Sandstone|37122|5|Briefly described|Table 1|||||||||
26871|Ripley Road Sandstone|37375|4|Described|p474|||||||||
26871|Ripley Road Sandstone|37456|6|Mentioned|p268|||||||||
26871|Ripley Road Sandstone|37463|6|Mentioned|p483|||||||||
26871|Ripley Road Sandstone|37616|6|Mentioned|p33|||||||||
26871|Ripley Road Sandstone|38074|5|Briefly described|Table 1|||||||||
26871|Ripley Road Sandstone|38076|6|Mentioned|Table 3|||||||||
26871|Ripley Road Sandstone|38306|6|Mentioned|p512|||||||||
26871|Ripley Road Sandstone|38307|4|Described|p522|||||||||
26871|Ripley Road Sandstone|38441|6|Mentioned|Map legend|Early Jurassic|Rhaetian|Rhaetian - Early Jurassic||||||
26871|Ripley Road Sandstone|39445|5|Briefly described|Table 10|||||||||
26871|Ripley Road Sandstone|39907|4|Described|p14|||Sedimentology||||||
26871|Ripley Road Sandstone|39943|6|Mentioned|Table 10A|||||||||
26871|Ripley Road Sandstone|40623|5|Briefly described|p107|||||||||
26871|Ripley Road Sandstone|41591|6|Mentioned|p18|||||||||
26871|Ripley Road Sandstone|41631|4|Described|p10|||See also Fig.2||||||
26871|Ripley Road Sandstone|41906|3|Fully described|Table 2 P16|||||||||
26871|Ripley Road Sandstone|42248|6|Mentioned|p397|||||||||
26871|Ripley Road Sandstone|42316|6|Mentioned|p8|||||||||
26871|Ripley Road Sandstone|42336|5|Briefly described|Table 1 P5|||||||||
26871|Ripley Road Sandstone|42405|6|Mentioned|Table 3 P.7|||||||||
26871|Ripley Road Sandstone|42463|6|Mentioned|Fig.3 P170|||||||||
26871|Ripley Road Sandstone|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundama Group).||||||15-JUL-04
26871|Ripley Road Sandstone|42869|5|Briefly described|Table 1, P33|||of Woogaroo Subgroup||||||
26871|Ripley Road Sandstone|42893|6|Mentioned|p11|||||||||
26871|Ripley Road Sandstone|42894|5|Briefly described|Fig.1 P20|||||||||
26871|Ripley Road Sandstone|43001|6|Mentioned|p122|||||||||
26871|Ripley Road Sandstone|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||12-APR-05
26871|Ripley Road Sandstone|43736|5|Briefly described|Table 1,p4|||||||||
26871|Ripley Road Sandstone|43910|4|Described|p1,3,10,16-18,Fig.2|||||||||
26871|Ripley Road Sandstone|44450|5|Briefly described|p27|||Underlying unit Raceview Formation. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|44734|14|Not recorded|p5,6,12,13,16,17,19|||||||||
26871|Ripley Road Sandstone|44774|2|Defined|p30-32||Late Triassic|Conformably overlies Raceview Formation. Upper limit hard to delineate, possible upward gradation into Marburg Sandstone.||||||
26871|Ripley Road Sandstone|44775|4|Described|p9||Late Triassic|||||||
26871|Ripley Road Sandstone|44776|14|Not recorded|p4||Late Triassic|||||||
26871|Ripley Road Sandstone|44884|4|Described|p2,3,Fig.1|||||||||
26871|Ripley Road Sandstone|45110|6|Mentioned|p83|||||||||
26871|Ripley Road Sandstone|48917|3|Fully described|p16|||See also p13. Stratigraphic table. Refers Staines (1964)||||||10-JUN-22
26871|Ripley Road Sandstone|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Arenite and conglomerate.||||||
26871|Ripley Road Sandstone|60281|5|Briefly described|p27, Fig.18 App 1|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Quartz sandstone, granule conglomerate.  Overlies the Raceview Formation; overlain by Gatton Sandstone.  Max. thickness: 150m. Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60993|4|Described|p4-5, p6 Fig. 2|Early Jurassic|LateTriassic|Of the Woogaroo Subgroup. Formely known as the "Helidon Sandstone" which is now interpreted as a facies variant within the unit. Overlies The Raceview Fm. Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60995|4|Described|p61, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp. Sandstone and quartz-rich granule conglomerate. Conformably overlies Raceview Fm; overlain by Calamia Mbr. Max. thick: 150m. Part of this unit is equivalent to "Olive Gap Fm". Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|60996|5|Briefly described|p72|||Quartzose sandstone forming an extensive blanket overlying the Raceview Formation. Geological Province: Clarence-Moreton Basin. Equivalent to Precipice Sandstone of the Surat Basin.||||||09-MAY-13
26871|Ripley Road Sandstone|60997|5|Briefly described|p139 Fig. 1|Sinemurian|Rhaetian|Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
26871|Ripley Road Sandstone|60999|5|Briefly described|p164, p172|Early Jurassic|Late Triassic|Of the Woogaroo Subgroup. Geological Province: Clarence-Moreton Basin. See also p172 Fig. 6.||||||
26871|Ripley Road Sandstone|61002|5|Briefly described|p201|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin. See also p199 Fig. 3.||||||
26871|Ripley Road Sandstone|61004|5|Briefly described|p232 Fig. 2|Jurassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|61005|5|Briefly described|p242|||See also p255 Figs. 23, 24 and 25. ||||||
26871|Ripley Road Sandstone|61006|5|Briefly described|p277, p289|Jurassic|Triassic|Formerly the Pillar Valley Fm. Quartzose sandstone (sheet-like braided-stream deposits) with potential as reservoir rocks. This unit is the most extensive potential reservoir in the basin. Geol. Prov: Clarence-Moreton Basin.||||||
26871|Ripley Road Sandstone|61310|5|Briefly described|p21, table C1 (p22-23)|||Of the Woogaroo Subgroup. Comprises a sandstone sequence with minor mudrock and conglomerate intervals, and minor coal.  Max. thickness: 500m. Geological Province: Clarence-Moreton Basin||||||
26871|Ripley Road Sandstone|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
26871|Ripley Road Sandstone|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with lower part of Landsborough Sandstone (Southern Nambour Basin), and Myrtle Creek Sandstone (Northern Nambour Basin).||Upper unit in Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Gatton Sandstone.||
26871|Ripley Road Sandstone|64856|5|Briefly described|p80, 81|||Moreton Basin. Grades laterally into Precipice Sandstone to west.| | ||||31-JAN-13
26871|Ripley Road Sandstone|65096|6|Mentioned|p373|||Clarence-Moreton Basin. Compared with the Jurassic sandstones east of the Kumbarilla Ridge and west of the Toowoomba Strait [accidently capitalised as Jurassic Sandstone] and the Precipice Sandstone of the Surat Basin, to the west.||||||
26871|Ripley Road Sandstone|66855|5|Briefly described|p956.|||Clarence-Moreton Basin.||||Unconformably overlies Evans Head Coal Measures.|Massive quartz sandstone.|
26871|Ripley Road Sandstone|67402|5|Briefly described|p165 tbl LPB1|Hettangian||Clarence-Moreton Basin. Deposited in a high energy environment. Approximately 70m thick. Sandstones are often reservoirs and potential reservoirs for the storage of carbon dioxide with an average porosity of 18% and an average permeability of 735 mD. See also p187, p188, p190, p190 fig CLM6, p192, p193, p195.||Woogaroo Subgroup||Overlies the Raceview Formation. Overlain by the Gatton Sandstone.|Massive, cross-bedded, fine to coarse-grained, sub-labile to quartzose sandstone.|
26871|Ripley Road Sandstone|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. Between 100-150m thick. In the onshore Clarence-Moreton Basin has great potential as a hydrocarbon reservoir rock. ||Woogaroo Subgroup||Overlies the Raceview Formation. Overlain by the Gatton Sandstone.||
26871|Ripley Road Sandstone|69594|4|Described|p519, p534-535, p543-547, p572|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Formerly the Helidon Sandstone. The Triassic-Jurassic boundary is at the base of this unit.||Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Gatton Sandstone. Merges with Precipice Sandstone in the Surat Basin.|Sheet-like, quartzose, cross-bedded sandstone.|
26871|Ripley Road Sandstone|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||||||
26871|Ripley Road Sandstone|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Aquifer: generally artesian.||Woogaroo Subgroup.||Overlies Raceview Formation. Is overlain by Koreelah Conglomerate Member (Gatton Sandstone).||
26871|Ripley Road Sandstone|71805|5|Briefly described|p75-p76|Sinemurian|Hettangian|Clarence-Moreton Basin. Referred to as the Ripley Road Formation on p75. This unit is a time equivalent to the Precipice Sandstone, Poolowanna Formation and the Helidon Formation.||Woogaroo Subgroup||Overlain by the Gatton Sandstone.||
26871|Ripley Road Sandstone|72298|6|Mentioned|p802|||Clarence-Moreton Basin. Has supplied small supplies of groundwater for irrigation.||||||
26871|Ripley Road Sandstone|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Triassic|Shown as located within the Clarence-Moreton Basin.||||Underlies Gatton Sandstone.||
26871|Ripley Road Sandstone|73570|6|Mentioned|p912 Fig.2, p913-914, p915 Fig.4|Rhaetian|Rhaetian|Clarence-Morton Basin.||||||
25680|Rishton Granodiorite|22847|3|Fully described|p 50||Late Silurian|||||||
25680|Rishton Granodiorite|23422|5|Briefly described|p176, p213 Table 6.8|Silurian|Silurian|Of Millchester Supersuite.||||||
25680|Rishton Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
25680|Rishton Granodiorite|23513|5|Briefly described|Map legend||Silurian|Palaeozoic Intrusive No 210. I-Type.||||||
25680|Rishton Granodiorite|24424|6|Mentioned|p526|||Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
25680|Rishton Granodiorite|42633|5|Briefly described|Table 1 P8|||Reserved.||||||
25680|Rishton Granodiorite|42750|6|Mentioned|p43|||||||||
25680|Rishton Granodiorite|43093|4|Described|Appendix 1|||Rb/Sr biotite age of 415+/-2Ma.||||||
25680|Rishton Granodiorite|43259|4|Described|Appendix 1,p30.||Late Silurian|Rb-Sr age is 415+/-2 Ma.||||||
25680|Rishton Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
25680|Rishton Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
25680|Rishton Granodiorite|50552|5|Briefly described|p1049 Fig.3||Late Silurian|In Lolworth-Ravenswood Terrane.||||||
25680|Rishton Granodiorite|62075|6|Mentioned|p15 Fig.7|Late Silurian|Late Silurian|Ravenswood batholith. Appears as Rishton granodiorite.||||||
40577|River Supersequence|62535|5|Briefly described|p672, p674|Statherian|Statherian|Isa Superbasin.|c.1640 - c.1630 Ma.|||||
40577|River Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Lynott and Barney Creek Formations, Teena and Emmerugga Dolostones, Leila Sandstone,  Myrtle Shale.|||
40577|River Supersequence|63866|5|Briefly described|p53-p54, p57|||Isa Superbasin.|||Includes the Teena Dolomite, Lynott Formation and the Riversleigh Formation.|||
40577|River Supersequence|65228|5|Briefly described|p16, p29, pp31-35, Figs.11, 19-22.|Statherian|Statherian|Best preserved in southern Lawn Hill Platform. Informally named after the Riversleigh Siltstone, which contains the maximum flooding surface. Comprises upper Umbolooga Subgroup and lower Batten Subgroup. Includes Teena Dolomite to top of Yalco Formation. Gamma ray log, lithology and facies detailed.|c.1640 Ma.|||Is overlain by Term Supersequence.||
40577|River Supersequence|65337|6|Mentioned|p33 Fig.27.|||Its beginning is marked by the Bullrush Conglomerate lying unconformably on Drummond Formation.||||Overlies Loretta Supersequence. Is overlain by Term Supersequence.||
40577|River Supersequence|66843|6|Mentioned|p38 Fig.10|||Said to be "informally" named.||||||
40577|River Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40577|River Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier.|~1645-1635 Ma.|McNamara Group.||Overlies Loretta Supersequence. Is overlain by Term Supersequence.||
40577|River Supersequence|68732|6|Mentioned|p159, p165 Fig.5|||Includes Riversleigh Formation and Shady Bore Formation.||||||
40577|River Supersequence|69591|5|Briefly described|p27, p43, p46-47, p54, p108|||Mount Isa Province. Includes Shady Bore Quartzite and Riversleigh Siltstone. Formed in a N-S series of depocentres.||||Overlies Loretta Supersequence. Is overlain by Term Supersequence.|Deeper-water clastic turbidites, with syn-sedimentary pyrite and Zn/Pb mineralisation.|
40577|River Supersequence|70897|5|Briefly described|p39, Fig.1.7.1,3,7|||Shows rapid thickness and lithofacies variations across regional fault systems.||||Is overlain by Term Supersequence.||
40577|River Supersequence|72912|5|Briefly described|p13, p33 Fig.12, p35 Fig.13.|Statherian|Statherian|Of Lawn Hill Hill Platform, Isa Superbasin. Shown to contain the highest Hydrogen Index (mg/g TOC) of all the units analysed for the South Nicholson, Fickling and McNamara Groups, at c. 265mg/g TOC indicated likihood of being oil prone (uniquely) as well as gas prone. Data from Jarrett et al. (2019).|c. 1640-1630 Ma|||Overlies Loretta Supersequence and underlies Term Supersequence.||
40577|River Supersequence|73144|4|Described|p4-5, p8-9, p11-12, p20, p25, p45, p49|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains four third order sequences labelled 5-8 representing those found on the southern flanks of the Murphy Inlier. All eight are reported on the central Lawn Hill Platform [see article for more detail on third order sequences]. Deposited in shallow-midouter shelfal environments, deep marine with some submarine fans and turbidites (Southgate et al., 2000). Drilling at Egilabria-4 has confirmed the presence of multiple thick and organic-rich shale gas intervals (Riversleigh Shale Gas Play). Potential source rock but modelled as overmature with 2% EqVR at Desert Creek 1 and Egilabria 1 wells. SHRIMP ages indicate it was probably deposited between 1645 and 1630 Ma (Krassay et al., 2000).  Contemporaneous deposition with the River Event, at ~1640 Ma associated with north-south extension.|1630-1645 Ma|||Includes Riversleigh Siltstone and Shady Bore Quartzite.|Siltstone, silty shale, lithic sandstone and sandstone.|
26281|River View Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
26281|River View Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 92. I-Type.||||||
26281|River View Granodiorite|42750|2|Defined|p45|Early Devonian|Late Silurian|||||||
26281|River View Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Silurian|Middle Silurian to Early Devonian age.||||||
26281|River View Granodiorite|43259|4|Described|Appendix 1,p21.|Early Devonian|Late Silurian|||||||
26281|River View Granodiorite|43933|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26281|River View Granodiorite|62521|6|Mentioned|p23|||See also Riverview Granodiorite. ||||||
81122|Riversleigh Limestones|69599|6|Mentioned|p580|||||||||
24472|Riversleigh Siltstone|22438|6|Mentioned|p549, Fig.12|||||||||
24472|Riversleigh Siltstone|22665|6|Mentioned|P231|||||||||
24472|Riversleigh Siltstone|22680|6|Mentioned|83,85,87|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||28-NOV-06
24472|Riversleigh Siltstone|23031|6|Mentioned|40|||Geological  province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Termite Range Formation.||||||28-NOV-06
24472|Riversleigh Siltstone|23072|5|Briefly described|p754|||||||||
24472|Riversleigh Siltstone|23362|6|Mentioned|339 Fig.2|||||||||
24472|Riversleigh Siltstone|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
24472|Riversleigh Siltstone|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlain by Termite Range Formation.||||||07-NOV-08
24472|Riversleigh Siltstone|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McNamara Group. Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23397|5|Briefly described|p472|Statherian|Statherian|Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23398|4|Described|p450|Statherian|Statherian|Of McNamara Group. Age: 1647+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23405|5|Briefly described|p565|||Of McNamara Group.||||||
24472|Riversleigh Siltstone|23406|5|Briefly described|p614|Statherian|Statherian|Of McNamara Group. Age: 1644+/-8Ma.||||||16-JUN-09
24472|Riversleigh Siltstone|23408|5|Briefly described|p513 Fig.2|||Of the McNamara Group.||||||28-NOV-06
24472|Riversleigh Siltstone|23409|4|Described|p541|Statherian|Statherian|Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
24472|Riversleigh Siltstone|23958|3|Fully described|p1135|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 2900m.||||||07-NOV-08
24472|Riversleigh Siltstone|23964|5|Briefly described|p1268|Proterozoic|Proterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.  Maximum thicknees: 3200m. See also p1269 Table 1.||||||01-OCT-08
24472|Riversleigh Siltstone|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
24472|Riversleigh Siltstone|24309|5|Briefly described|p1013|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24472|Riversleigh Siltstone|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Shady Bore Quartzite. Overlain by Termite Range Formation. Age: 1644-1636 Ma. Geological Province: Lawn Hill Platform.||||||
24472|Riversleigh Siltstone|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|37459|2|Defined|p431|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
24472|Riversleigh Siltstone|38237|4|Described|p129|||||||||
24472|Riversleigh Siltstone|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|38310|6|Mentioned|p237|||||||||
24472|Riversleigh Siltstone|38348|4|Described|p15|||||||||
24472|Riversleigh Siltstone|38584|6|Mentioned|p22|||||||||
24472|Riversleigh Siltstone|39445|5|Briefly described|Table 2|||||||||
24472|Riversleigh Siltstone|39497|6|Mentioned|p13|||See also Fig.4||||||
24472|Riversleigh Siltstone|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Top unit in McNamara Group. Laminated fine siltstone and shale with thin interbeds of coarse siltstone and fine sandstone.||||||15-JUN-06
24472|Riversleigh Siltstone|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|39925|6|Mentioned|Fig.9|||||||||
24472|Riversleigh Siltstone|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|40221|4|Described|p19|||||||||
24472|Riversleigh Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
24472|Riversleigh Siltstone|43486|5|Briefly described|21||Paleoproterozoic|Of the Upper McNamara Group.||||||07-NOV-08
24472|Riversleigh Siltstone|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
24472|Riversleigh Siltstone|45166|5|Briefly described|p30|||See also p71.||||||28-NOV-06
24472|Riversleigh Siltstone|47083|5|Briefly described|p18||Proterozoic|Of McNamara Group. Underlain by Shady Bore Quartzite.||||||28-NOV-06
24472|Riversleigh Siltstone|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: c.1644 Ma. Conformably overlies Shady Bore Siltstone, confromably overlain by Termite Range Formation. Geological Province: Western Fold Belt.||||||01-OCT-08
24472|Riversleigh Siltstone|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Siltstone, carbonaceous siltstone and shale, massive to blocky, silicified very fine sandstone; dolomite, dolomitic siltstone, medium sandstone. Overlies Shady Bore Formation.||||||01-OCT-08
24472|Riversleigh Siltstone|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Termite Range Formation, underlain by Shady Bore Quartzite.||||||
24472|Riversleigh Siltstone|61736|5|Briefly described|p674|||Of the McNamara Group. Age: 1644+/-8Ma.||||||
24472|Riversleigh Siltstone|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
24472|Riversleigh Siltstone|62084|4|Described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Riversleigh Slst.|1647+/-8 Ma U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Variably dolomitic organic siltstones and shales.|
24472|Riversleigh Siltstone|62535|5|Briefly described|p672, p674|Statherian|Statherian|Lawn Hill Platform. Hosts the Grevillea Pb-Zn-Ag prospect. Lithology not specified on p672.|1644 +/- 8 Ma.|McNamara Group.||||
24472|Riversleigh Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Termite Range Formation and Mount Les Siltstone. Geological Province: Isa Superbasin. Consists of siltstone.||||||30-SEP-08
24472|Riversleigh Siltstone|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of River Supersequence. Age: 1644+/-8 and 1640+/-7Ma. Geological Province: Isa Superbasin. Consists of conglomerates and fine-grained arenites.||||||07-FEB-11
24472|Riversleigh Siltstone|63113|6|Mentioned|p1214 Fig.2, p1219 Fig.8, p1225 Fig.13. |||Part of River supersequence. Shown as L.Riv.Sltst, M.Riv.Sltst, U.Riv.Sltst with their different lithologies, in Fig.2.|c.1644 Ma.|Of the McNamara Group||Overlies Shady Bore Quartzite or Lady Loretta Formation. Is overlain by Lawn Hill Formation or ?unconformably by Termite Range Formation.||
24472|Riversleigh Siltstone|63114|5|Briefly described|p1253 Fig.2, p1256, p1268. |||Isa superbasin. Appears only as Riversleigh in Fig.2. Hosts the Flat Tyre Zn-Pb prospect. Dolomite was added to this unit during mineralization.||Of the River supersequence.||||
24472|Riversleigh Siltstone|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
24472|Riversleigh Siltstone|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed.||||||
24472|Riversleigh Siltstone|64575|6|Mentioned|p665|||||||||
24472|Riversleigh Siltstone|65228|5|Briefly described|p16, p33, Fig.04.|Statherian|Statherian|Mid-shelf to deep marine, commonly turbiditic clastic facies. Contains the maximum flooding surface of the River Supersequence, informally named after this unit.|1644 +/- 8 Ma (SHRIMP).|||||
24472|Riversleigh Siltstone|65337|5|Briefly described|p33 Fig.27.|||Correlative with Plain Creek Formation.|1647 +/- 8 to 1630 +/- 5 Ma (Page et al. 2000).|||Overlies Shady Bore Quartzite. Is overlain by Termite Range Formation.||
24472|Riversleigh Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p9, p11. Mount Isa Inlier, Isa Superbasin. Camooweal - Murphy and Century Domains, Mount Isa Inlier. |1644 +/- 8 Ma.|McNamara Group.|||Laminated fine siltstone and shale with thin interbeds of coarse siltstone and fine sandstone.|
24472|Riversleigh Siltstone|68542|6|Mentioned|p6|||||Upper McNamara Group||Overlies Shady Bore Quartzite, disconformably overlain by Termite Range Formation||
24472|Riversleigh Siltstone|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Grevillea Zn-Pb-Ag deposit.||Upper McNamara Group.||Overlies Shady Bore Quartzite. Is overlain by Termite Range Formation.||
24472|Riversleigh Siltstone|69591|4|Described|p43 Fig.2.31, p46-47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Part of River Supersequence. Up to 3300m thick. The sandstone and quartzite beds are lowstand deposits: fluvial channels, shoreface deposits and deeper-marine turbidites and sand-rich submarine fans. See also reference to Riversleigh Formation (p108).|1644 +/- 7 Ma (MDA: Page et al., 2000).|McNamara Group.||Equivalent to Mount Les Siltstone.|Mainly laminated fine siltstone and shale, with several sandstone and locally quartzite interbeds.|
24472|Riversleigh Siltstone|69673|6|Mentioned|p54|||High enough TOC to be considered valid source rock.||||Correlated with Plain Creek Formation||
24472|Riversleigh Siltstone|70897|6|Mentioned|Fig.1.7.7|||Isa Superbasin.||||||
24472|Riversleigh Siltstone|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1647+/-8 Ma.||||Shale.|
24472|Riversleigh Siltstone|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
24472|Riversleigh Siltstone|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72526|5|Briefly described|p8 Fig.1.3, p10.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1647 +/- 8 Ma, 1644 +/- 8 Ma|McNamara Group||Conformably overlies Shady Bore Quartzite and underlies Termite Range Formation.||
24472|Riversleigh Siltstone|72527|6|Mentioned|p132.|Statherian|Statherian|Tuff ages considered 'reasonably firm' age constraints. Variation on Riversleigh Formation.|1647+/-8 Ma. 1644+/-8 Ma|McNamara Group||Correlative with Plain Creek Formation, Termite Range Formation.|Includes tuffaceous horizons.|
24472|Riversleigh Siltstone|72912|4|Described|p5 Fig.3, p14, p32, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the Lawn Hill Platform of the Isa Superbasin, Mount Isa Province, and the East part of the South Nicholson Basin. Also shown as Riversleigh Formation p32, 45. See also p45-46, p49.||McNamara Group||Overlies Shady Bore Quartzite and underlies Termite Range Formation.|Includes organic rich siltstone and shales.|
24472|Riversleigh Siltstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p22, 23, 26|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in 3 wells in this study.  Mineral composition shows majority quartz, microcline, muscovite and dolomite.|1644 +/- 5 Ma|McNamara Group||Overlies Shady Bore Quartzite and underlies Termite Range Formation.|Includes organic rich siltstone.|
24472|Riversleigh Siltstone|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
24472|Riversleigh Siltstone|73042|5|Briefly described|p1, p4, p6, p11-13|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Re-Os age overlaps with existing zircon depositional age constraints including zircon U-Pb geochronology of tuff and tuffaceous intervals (ca 1647-1644 Ma, Page et al., 2000); the unit is an important source rock in the Isa Superbasin.|1608 +/- 40 Ma Re-Os|McNamara Group||Conformably underlain by the Shady Bore Quartzite. Unconformably overlain by the Termite Range Formation.|Siltstone, shale, sandstone, dolomitic and carbonaceous siltstone.|23-JUN-22
24472|Riversleigh Siltstone|73098|6|Mentioned|p4, p7, p25|||Lawn Hill Platform. Organic petrolography performed on four samples from the Amoco DDH 83-1 well. [See report for bitumen/maceral description].|||||Includes weakly laminated dark brown to dark grey shale.|
24472|Riversleigh Siltstone|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. River Supersequence. Aquifer. Potential shale gas/oil play. Includes oil show and gas show.||McNamara Group||Unconformably underlain by Lady Loretta Formation. Overlain by Termite Range Formation.||
24472|Riversleigh Siltstone|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1647+/-8 Ma crystallisation of volcanic rock||||Carbonates, siliciclastics.|
38885|Riverston Granodiorite|24489|5|Briefly described|Map Legend|Triassic|Permian|||||||
38885|Riverston Granodiorite|68008|4|Described|p426-428|Triassic|Permian|Previously mapped as an undifferentiated Permian to Triassic intrusion by Dear et al. (1971). A rectangular body, 3 x 2km, located 8km ESE of Calliope, at the N edge of Lake Awoonga. Named after Riverston Creek. Geophysics briefly described. Hosts old gold workings.||||Intrudes Wandilla Formation.|Grey, equigranular to porphyritic, biotite granodiorite to diorite; some trondhjemite; numerous E-W trending bodies of rhyolite and microgranite which are more altered than the granodiorite and extend beyond it.|
38885|Riverston Granodiorite|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Porphyritic biotite granodiorite to diorite; includes altered and fractured microgranite and porphyritic rhyolite, breccia.|
34671|Riverview Suite|22847|5|Briefly described|p 13|||||||||
34671|Riverview Suite|23422|5|Briefly described|p175, p213 Table 6.8|||Of Millchester Supersuite.||||||
34671|Riverview Suite|62521|5|Briefly described|p55|||Probably misspelt - should be River View Suite. Includes River View Granodiorite. Geological Province: Ravenswood Batholith.||||||14-JAN-08
34671|Riverview Suite|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.||Millchester Supersuite.|||Mostly medium-K granodiorites to tonalites.|
30013|Roaring Meg Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|266-234 Ma.|Unit in Collingwood Group.||||
30013|Roaring Meg Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|Of Cooktown Supersuite. Age: 259 - 266Ma.||||||02-JUN-09
30013|Roaring Meg Granite|43070|2|Defined|p88|Late Permian||of Cooktown Supersuite.||||||
30013|Roaring Meg Granite|43625|4|Described|p56,126,Appendix 7|||||||||
30013|Roaring Meg Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic, (tourmaline-) cordierite(altered)-biotite granite.||||||
30013|Roaring Meg Granite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Roaring Meg Suite (Cooktown Supersuite). Age: 266-259Ma (Rb-Sr, est.). S-type. Mod'ly to highly porphyritic, med.-coarse-gr. Tourmaline-biotite granite; pegmatitic patches common; accessory cordierite (altered) etc. - more lithol. detail included||||||07-FEB-11
30013|Roaring Meg Granite|69593|5|Briefly described|p479, p481 Fig.6.5 (a)|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Roaring Meg Suite.|||S-type granitoids.|
36726|Roaring Meg Suite|23423|5|Briefly described|Table 7.1 p240|||Of Collingwood Group.||||||
36726|Roaring Meg Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains Bourgamba and China Camp Microgranites and Roaring Meg Granite. S-types.||||||07-FEB-11
36726|Roaring Meg Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Roaring Meg Granite; Bourgamba, China Camp Microgranites.||S-type granitoids.|
38870|Robert Granite|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38870|Robert Granite|24489|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38870|Robert Granite|24615|5|Briefly described|CD|Triassic|Triassic|[Rggo].   Pink fine to medium-grained hornblende granite and quartz monzonite with granophyric groundmass and miarolitic cavities;  arfvedsonite granite.||||||12-NOV-15
38870|Robert Granite|67203|5|Briefly described|p4, p7, p11|Triassic|Triassic||230.2 +/- 3.2 Ma (Cross, unpublished).||||Medium-grained, porphyritic hornblende monzonite or quartz monzonite.|
38870|Robert Granite|67874|6|Mentioned|p28|Late Triassic|Late Triassic|Yarrol Province.||||||
38870|Robert Granite|68008|2|Defined|p2, p6, p8, p11, p48, p50, p69-71, p73|Late Triassic|Late Triassic|See also p77, p80, p88-110, p117, p122, p132, p140, p143, p158, p162, p188, p194, p209, p213, p215-217, p246, p254, p261, p270, p275, p279, p307, p357, p402-403, p405-409, p411, p529, p637. Previously, largely mapped as Muncon Volcanics by Dear et al. (1971). An oval intrusion 8 x 5km, centred 10km W of Many Peaks township. Named after Mount Robert. The type area is the headwaters of Prizemans Creek. Resistant unit; forms prominent peak (Mount Robert) and steeply dissected plateau. Geophysics described. Contains alkali amphiboles; within-plate granite field and tends towards A-type. A discrepancy between ages of this unit, and the Littlemore Granodiorite and Lawyer Granite it intrudes, is discussed.|230.2 +/- 3.7 Ma (U-Pb zircon; Fanning, 2012)|Glassford Igneous Complex.||Intrudes Rule Gabbro, Littlemore Granodiorite and Lawyer Granite.|Altered, pink to greyish pink, medium-grained, sparsely porphyritic, leucocratic granite to quartz monzonite, commonly with miarolitic cavities and a granophyric groundmass. Mineralogy elaborated. A-type.|
38870|Robert Granite|68679|5|Briefly described|p343, p431|Late Triassic|Late Triassic|Western side of the Boyne River valley, Bundaberg-Agnes Water-Biloela region. Forms a steeply dissected plateau.|230.2 +/- 3.7 Ma (SHRIMP U-Pb: Fanning, 2012).|Glassford Igneous Complex.|||A-type. Pink, fine- to medium-grained hornblende granite and quartz monzonite with granophyric groundmass and miarolitic cavities; arfvedsonite granite.|
38870|Robert Granite|71592|5|Briefly described|Appendix A.||||230+/-3.7 Ma (SHRIMP U-Pb zircon).||||Granite.|
38870|Robert Granite|73450|4|Described|p.10-11, 13-15, 23, 28,35,37,60,62,64,66|Norian|Carnian|Defined by Murray et al. (2012). Forms an ovoid intrusion west of Many Peaks township. Yielded a U-Pb SHRIMP zircon age of 230.2 +/- 3.7 Ma (Murray et al., 2012).|230.2 +/- 3.7 Ma U-Pb SHRIMP|Glassford Igneous Complex||Intrudes Littlemore Granodiorite, Rule Gabbro, and Lawyer Granite.|Altered, pink to greyish pink, medium-grained, sparsely porphyritic, leucocratic granite to quartz monzonite, commonly with miarolitic cavities and a granophyric groundmass.|
37883|Roberts Creek Suite|23291|5|Briefly described|p96 Tb. 3.11, p100 Tb. 12|Late Carboniferous|Late Carboniferous|Of the O'Brien's Creek Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
25745|Robertson River Subgroup|22533|6|Mentioned|p55|||In Georgetown Region.||||||16-JAN-07
25745|Robertson River Subgroup|23085|5|Briefly described|p670|||||||||
25745|Robertson River Subgroup|23220|6|Mentioned|p17|||||||||
25745|Robertson River Subgroup|23291|5|Briefly described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Originally mapped as Robertson River Metamorphics. Of the Etheridge Group. Geological Province: Georgetown Region.||||||08-JUL-15
25745|Robertson River Subgroup|23429|5|Briefly described|p435|||||||||
25745|Robertson River Subgroup|23431|6|Mentioned|p532|||||||||
25745|Robertson River Subgroup|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25745|Robertson River Subgroup|23510|5|Briefly described|Map Legend||Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
25745|Robertson River Subgroup|23616|5|Briefly described|Table 1C p15|||Metamorphics component probably equivalent to McDevitt Metamorphics. Of Etheridge Group. In the Georgetown Inlier.||||||16-JAN-07
25745|Robertson River Subgroup|23713|5|Briefly described|p11|||Correlate with rocks in the McDevitt Metamorphics||||||
25745|Robertson River Subgroup|24485|5|Briefly described|p1, p15 Tb.1|Mesoproterozoic|Mesoproterozoic|Parent: Etheridge Group. Age: ~1700-1655Ma.||||||16-JAN-07
25745|Robertson River Subgroup|38714|1|Redefined|p183|Mesoproterozoic|Mesoproterozoic|||||||
25745|Robertson River Subgroup|38715|6|Mentioned|p191|||||||||
25745|Robertson River Subgroup|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
25745|Robertson River Subgroup|39924|6|Mentioned|p341|||||||||
25745|Robertson River Subgroup|41272|5|Briefly described|M 1of1 B05|||See also M 1of1 F04||||||
25745|Robertson River Subgroup|41975|6|Mentioned|p431|||||||||
25745|Robertson River Subgroup|42199|6|Mentioned|FIG.1 P279|||||||||
25745|Robertson River Subgroup|43060|6|Mentioned|p28|||||||||
25745|Robertson River Subgroup|43083|5|Briefly described|p27|||Of the Etheridge Group. Geological province: Georgetown Province.||||||17-JUN-09
25745|Robertson River Subgroup|43664|4|Described|p22|||||||||
25745|Robertson River Subgroup|43793|5|Briefly described|p333|||||||||
25745|Robertson River Subgroup|50198|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Consists of the Daniel Creek Formation, Corbett Formation, Lane Creek Formation.||||||18-JUN-15
25745|Robertson River Subgroup|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Consists of Daniel Creek Formation, Dead Horse Metabasalt, Corbett Formation, Lane Creek Formation, Townley Formation.||||||18-JUN-15
25745|Robertson River Subgroup|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group. Intruded by the Cobbold Metadolerite. Includes: Lane Creek Formation, Corbett Formation, Dead Horse Metabasalt, Daniel Creek Formation.||||||18-JUN-15
25745|Robertson River Subgroup|50211|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Etheridge Group.||||||07-NOV-08
25745|Robertson River Subgroup|50537|5|Briefly described|p2.3, 2.4|||Intruded by Forsayth Supersuite. Geological Province: Georgetown Inlier.||||||
25745|Robertson River Subgroup|50595|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.||||||07-NOV-08
25745|Robertson River Subgroup|61258|5|Briefly described|p386, p387 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Etheridge Grp in east. Grades into Bernecker Creek and Daniel Creek Formations towards west. Med- to high-grade rocks (biotite, hornblende and hornblende-diopside (calc-silicate) gneiss, mica schist, quartzite,  migmatite). Geol.Prov: Georgetown Inlier||||||07-NOV-08
25745|Robertson River Subgroup|64726|6|Mentioned|p83 Fig.2.|||||||||
25745|Robertson River Subgroup|65887|5|Briefly described|p40 Fig.1, p41-42|Statherian|Paleoproterozoic|Of Etheridge Group. Includes Daniel Creek Formation, Dead Horse Metabasalt, Corbett Formation and Lane Creek Formation. Greenschist to amphibolite facies Fe-rich mafic rocks.||||||
25745|Robertson River Subgroup|66529|6|Mentioned|p5 ||||1665-1620 Ma.|Unit in Etheridge Group.||||
25745|Robertson River Subgroup|66800|5|Briefly described|p926 Table 1, p928, p932|||||Unit in Etheridge Group.|Includes Daniel Creek, Corbett and Lane Creek Formations and Dead Horse Metabasalt.||Metadolerite and metagabbro sills and small stocks common.|
25745|Robertson River Subgroup|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.|Includes Lane Creek Formation.|||13-MAY-15
25745|Robertson River Subgroup|68352|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.|Includes Daniel Creek, Corbett and Lane Creek Formations.|Is intruded by Cobbold Metadolerite.|Mica schist, quartzite, calc-silicate rocks, mudstone, siltstone.|
25745|Robertson River Subgroup|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.|Includes Daniel Creek, Corbett, Lane Creek and Townley Formations; Dead Horse Metabasalt.|Conformably overlies Bernecker Creek Formation. Is intruded by Cobbold Metadolerite.||
25745|Robertson River Subgroup|68354|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.|Includes Daniel Creek, Corbett and Lane Creek Formations.|Is intruded by Cobbold Metadolerite.||
25745|Robertson River Subgroup|68357|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Etheridge Group.|Includes Bernecker Creek, Daniel Creek, Corbett and Lane Creek Formations; Dead Horse Metabasalt.|Is intruded by Cobbold Metadolerite.||
25745|Robertson River Subgroup|68415|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Of the Etheridge Group.|Includes Lane Creek Formation, Corbett Formation, Dead Horse Metabasalt, Daniel Creek Formation.|Intruded by Cobbold Metadolerite.||08-SEP-14
25745|Robertson River Subgroup|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. This unit, as well as the Cassidy Creek, Juntala and McDevitt Metamorphics, are all mapped under the symbol, -Per.||Unit in Etheridge Group.||Conformably overlies Bernecker Creek Formation, Dargalong and  Einasleigh Metamorphics.||
25745|Robertson River Subgroup|69582|5|Briefly described|p76|||Etheridge Province. Estimated to be between 1000-2000m thick. Intersected in GSQ Georgetown 8-9R.||Etheridge Group|Includes the Daniel Creek Formation, Dead Horse metabasalts, Corbett Formation and the Lane Creek Formation.|Overlain by the Townley Formation.||
25745|Robertson River Subgroup|69591|5|Briefly described|p61, p64-65|Paleoproterozoic|Paleoproterozoic|White (1965). Forsayth Subprovince, Etheridge Province.||Etheridge Group.|Daniel Creek Formation, Dead Horse Metabasalt, Corbett Formation, Lane Creek Formation.|Overlies Bernecker Creek Formation. Probably correlative with McDevitt Metamorphics.||
22762|Robey Range Granite|22847|3|Fully described|p 57|Permian|Carboniferous|||||||
22762|Robey Range Granite|23422|5|Briefly described|p218 Table 6.12|||Of Bogie Suite.||||||
22762|Robey Range Granite|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22762|Robey Range Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 201. I-Type.||||||
22762|Robey Range Granite|43093|4|Described|Appendix 1|Permian|Carboniferous|||||||
22762|Robey Range Granite|43259|4|Described|Appendix 1,p29.|Permian|Carboniferous|||||||
22762|Robey Range Granite|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
22762|Robey Range Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Bogie Suite.||||
39584|Robyndale Adamellite|23799|6|Mentioned|p86|Triassic|Triassic|Of Creaser (1984).  Within the core of the Eskdale Igneous Complex.   Geological Province: Yarraman Subprovince (Wandilla Province).||||||
22767|Rock Hole Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
22767|Rock Hole Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age:  304+/-4 Ma, Rb-Sr. of Boonmoo Volcanic Subgroup.||||||
22767|Rock Hole Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. 126. I-Type.||||||
22767|Rock Hole Rhyolite|23616|5|Briefly described|Table 3 p48||Carboniferous|Age: 304+/-4 Ma (Rb-Sr). Of Boonmoo Volcanic Subgroup.||||||
22767|Rock Hole Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group||||||
22767|Rock Hole Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).  Intensely welded, massive rhyolitic ignimbrite.  Age: 304+/-4Ma.||||||15-JUN-06
22767|Rock Hole Rhyolite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|of Boonmoo Volcanic Subgroup. Age is 304+/-4 Ma.||||||
22767|Rock Hole Rhyolite|43567|5|Briefly described|Table 2,p400|||||||||
22767|Rock Hole Rhyolite|43625|6|Mentioned|p36|||Age: Late Carboniferous (304-305 Ma)||||||
22767|Rock Hole Rhyolite|43626|2|Defined|p29||Late Carboniferous|between 306+/-3 Ma and 304+/-4 Ma||||||
22767|Rock Hole Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22767|Rock Hole Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group). Ages: 304+/-4Ma. Lithology for the subgroup included.||||||07-FEB-11
22767|Rock Hole Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Boonmoo Volcanic Subgroup.|||Pale pinkish grey, pink, purplish pink, or salmon, intensely welded, moderately to very crystal-rich, leucocratic, biotite-bearing, rhyolitic ignimbrite.|
39576|Rock Point Granodiorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
36255|Rock of Ages Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36255|Rock of Ages Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 280. I-Type.||||||
36255|Rock of Ages Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36255|Rock of Ages Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Ck Supersuite). Fine-grained granophyric biotite granite. I-type.||||||07-FEB-11
41096|Rockdale Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41096|Rockdale Granite|65388|2|Defined|p272-273, p262, 236, 253, 256, 331|Late Carboniferous|Late Carboniferous|Auburn Arch. Intrudes Torsdale Volcanics. May post-date Glen View Quartz Monzodiorite, J P Granite. Intruded by the Mungunal Granite which has yielded a K-Ar biotite age of 307+/- 6Ma (Webb & McDougall, 1968). K-Ar (hornblende) age of 300+/- 6Ma (Webb & McDougall, 1968; adjusted). May pre-date Nine Mile Granite, Ravenscraig Gabbro. Very pale pink to very pale brown, fine to medium-grained, slightly porphyritic hornblende-biotite monzogranite||||||
41096|Rockdale Granite|68679|5|Briefly described|p407-408, p419|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age relationships with several other units given.|300 +/- 6 Ma (K-Ar: Webb and McDougall, 1968).|||Intrudes Torsdale Volcanics. Is intruded by Mungunal Granite and Ravenscraig Gabbro.|Pink to brown, fine- to medium-grained, slightly porphyritic hornblende-biotite monzogranite with phenocrysts of alkali feldspar.|
36416|Rockingham Bay Granite|23617|4|Described|Table 2 p18||Carboniferous|Also see p22. Of Oweenee Supersuite Kennedy Province.||||||
36416|Rockingham Bay Granite|23618|5|Briefly described|map legend||Carboniferous|||||||
36416|Rockingham Bay Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
40443|Rockpool Granite|60659|5|Briefly described|p18|||Comprises quartz monzonite and granodiorite.||||||07-FEB-11
40443|Rockpool Granite|64852|5|Briefly described|Map legend|Permian|Carboniferous|Grey to pink, fine- to medium-grained, equigranular to weakly porphyritic, hornblende-biotite granodiorite and monzogranite.||||||
40443|Rockpool Granite|70740|5|Briefly described|p129|||Outcrop characteristics and distribution briefly discussed. ||||Intrudes the Saint Anns Formation and Scartwater Formation.|Fine to medium grained, equigranular to weakly porphyritic, hornblende-biotite granodiorite and monzogranite.|
36195|Rocky Islets Granite|23512|5|Briefly described|Map Legend||Early Permian|||||||
28033|Rocky King Granite|23420|4|Described|p 152 table 4.8||Early Devonian|In the Lukinville Suite of the Kintore Supersuite.||||||
28033|Rocky King Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
40135|Rocky Point Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgar].  Grey to pinkish-grey medium-grained biotite-hornblende granodiorite, locally with poikilitic K feldspar.||||||
40135|Rocky Point Granodiorite|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
40135|Rocky Point Granodiorite|68008|2|Defined|p330-331, p334-335, p372-373, p375-376|Early Triassic|Early Triassic|See also p378-384, p386-387, p389, p628-629. New name, after Rocky Point Mountain. Forms an ovoid pluton 20 x 13km, 40km NNE of Biloela, surrounding Dumgree Tonalite. The type area is along Bell Creek and its tributaries NE of Mount Buckland. Forms varied topography (described). Geophysics described; contrasted with other constituents of the Igneous Complex. Geochemistry described; similar to Umbrella Granodiorite, and contrasted with Bocoolima Granodiorite, Wyalla Granite and Dumgree Tonalite. K-Ar hornblende and biotite ages respectively by Webb and McDougall (1968). Hosts the Mount Rainbow Goldfield. Geophysics modelled. Is intruded by Redshirt and Wyalla Granites, and ?Dumgree Tonalite.|247 +/- 5 Ma and 244 +/- 5 Ma.|Galloway Plains Igneous Complex.||Intrudes Youlambie, Three Moon Conglomerates; Rockhampton Group; Balaclava, Mount Alma, Raspberry Creek Formations, and probably Bocoolima Granodiorite and Sawnee Gabbro. See Comments.|Biotite-hornblende granodiorite; lesser augite-biotite-hornblende tonalite. A local body of pyroxene-biotite-hornblende quartz diorite. Local periphery of strongly magnetic diorite and gabbro.|
40135|Rocky Point Granodiorite|68679|5|Briefly described|p425, p427|||Yarrol Province. Western third of the Galloway Plains Igneous Complex. Forms a single large, ovoid, N-S pluton with the Dumgree Tonalite. Geochemistry briefly described. This and another very similar age by the same authors were probably reset by ~251 Ma intrusions.|244 +/- 5 Ma (K-Ar: Webb and McDougall, 1968).|||Intrudes Youlambie, Three Moon Conglomerates; Rockhampton Group; Balaclava, Mount Alma and Raspberry Creek Formations; Wyalla Granite; possibly Sawnee Gabbro.|Biotite-hornblende granodiorite.|
37888|Rocky Whistler Suite|23291|5|Briefly described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
41099|Rockybar Granodiorite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41099|Rockybar Granodiorite|65388|2|Defined|p273-274, p236 Fig. 81|Early Triassic|Late Carboniferous|Presumed to intrude the Torsdale Volcanics beneath the cover of overlying Cainozoic deposits. Age poorly constrained, but post dates Torsdale Volcanics. Could be late Carboniferous to early Permian like other granitoids to the north or late Permian to Early Triassic like the nearby Flat Range Granodiorite. Pale grey to pale pink, fine to medium-grained, slightly porphyritic biotite-hornblende granodiorite. ||||||
41099|Rockybar Granodiorite|68679|5|Briefly described|p408|Middle Triassic|Late Carboniferous|Auburn Subprovince, New England Orogen. Age uncertain: Late Carboniferous to early Permian or late Permian to Middle Triassic.||||Intrudes Torsdale Volcanics.|Grey, fine- to medium-grained, slightly porphyritic biotite-hornblende granodiorite.|
70390|Rodds Peninsula Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70390|Rodds Peninsula Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink, fine to medium-grained, uneven-grained to porphyritic, leucocratic biotite monzogranite; locally granophyric, miarolitic; intruded by abundant basalt dykes.|
70390|Rodds Peninsula Granite|68679|5|Briefly described|p428, p432|Late Triassic|Late Triassic|Northern New England Orogen; Agnes Waters area.|||||Pink, fine- to medium-grained to porphyritic, leucocratic biotite monzogranite; locally granophyric and miarolitic; abundant basalt dykes.|
69613|Roeburne Volcanics|61155|5|Briefly described|p20|Late Oligocene|Early Oligocene|In the Rockhampton-Gladstone area.||||||
80680|Rokeby Quartz Monzodiorite|71849|3|Fully described|p3-4, p8, p14, p18, p65-66, p115-120|Devonian|Devonian|See also p151, p170-172, p176-177, p195. New name, after Rokeby Road. Formerly mapped partly as Flyspeck Granodiorite and partly as Kintore Adamellite. Two discrete outcrops separated by the younger Keane Granite, ~17-22km W of Coen airport. Type area is around MGA 709832 8482440. Interpreted to have crystallised at depths >20-25 km. Geophysics described; geochemistry and lithologies described in detail, with photomicrographs. This age (by Lewis et al. in prep.) is within error of previous ages of the Flyspeck Supersuite. Unassigned.|409 +9/-4 Ma (U-Pb SHRIMP zircon).|||Interpreted to intrude Yarraden Schist and to be intruded by Keane Granite. Is overlain nonconformably by Gilbert River Formation.|Mainly even-grained to slightly porphyritic (in plagioclase) hornblende-biotite quartz monzodiorite to granodiorite?. Contains magmatic zoned epidote grains with allanite cores. Calc-alkaline I-type. Deeply weathered; very poorly exposed.|
80680|Rokeby Quartz Monzodiorite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||||Mainly dark grey medium-grained even-grained to slightly porphyitic hornblende-biotite quartz monzodiorite to granodiorite; minor fine-grained (hornblende-)biotite tonalite; deformed with a poorly to moderately developed, locally gneissic, foliation.|
80680|Rokeby Quartz Monzodiorite|73387|4|Described|p1-2, p25-30|Early Devonian|Early Devonian|Pama Igneous Association. Constitutes a small, poorly exposed, and deeply weathered calc-alkaline I-type pluton northwest of Coen. Forms scattered, low, rounded boulders in gently undulating country. Geochemically distinct from the nearby Blue Mountains Supersuite and Flyspeck Supersuite. New zircon U-Pb SHRIMP magmatic crystallisation age of 407.7 + 3.1 / 3.6 Ma published herein. Emplaced at the same time as the other members of the association in the Cape York Peninsula Batholith.|407.7 + 3.1 / -3.6 Ma U-Pb SHRIMP|||Intruded by Keane Granite (Kintore Supersuite).|Variably deformed (and locally gneissic) dark grey, medium-grained (average grain-size c. 1.5 mm), equigranular to slightly porphyritic (in plagioclase) hornblende-biotite quartz monzodiorite.|
73044|Rokeby beds|61392|5|Briefly described|p164 Fig. 1|Early Permian|Early Permian|||||||07-FEB-11
30353|Rokehurst Creek rhyolite|23291|5|Briefly described|p98 Tb. 3.11|Late Carboniferous|Carboniferous|Informal name. Of the Purkin Batholith intruding the Etheridge Group. Age: 311+/-5 Ma (K-Ar, Richards et al). Geological Province: Georgetown Region.||||||08-JUL-15
30353|Rokehurst Creek rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 48. Assumed to be I-Type.||||||
30353|Rokehurst Creek rhyolite|43259|6|Mentioned|Appendix 1,p4 p18|||Related to McDougall Creek rhyolite?||||||
23942|Rolfe Creek Schist|22557|6|Mentioned|p567,569|||||||||
23942|Rolfe Creek Schist|23078|5|Briefly described|p708|||||||||
23942|Rolfe Creek Schist|42747|5|Briefly described|p33, Fig.3|||of Anakie Metamorphic Group||||||
23942|Rolfe Creek Schist|43204|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Neoproterozoic or Early Cambrian. Anakie Inlier||||||23-DEC-11
23942|Rolfe Creek Schist|43213|4|Described|p8, p20-23, p25-26, p35-37, p130-140|||See also p203, p236, p240, p245. Named after Rolfe Creek. Type area in Slaty Creek-Expedition Creek area is described. Geophysical properties described. Deformation structures and chemical analyses detailed.||Unit in Anakie Metamorphic Group.||Overlies Bathampton Metamorphics. Is overlain by Monteagle Quartzite. Is intruded by Sunny Park and Kilmarnock Granodiorites. Is faulted against Silver Hills Volcanics.|Consists entirely of strongly foliated, fine-grained, grey to green, mica schist grading into phyllite. Lacks quartzite and greenstone.|
23942|Rolfe Creek Schist|43861|2|Defined|25; Fig1p26; p28-29|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group||||||
23942|Rolfe Creek Schist|66851|5|Briefly described|p917 Fig.2, pp918-922.|||Double closures suggest that folding of F1 hinge has occurred with subsequent refolding by F3.||Unit in Anakie Metamorphic Group.||||18-JAN-17
23942|Rolfe Creek Schist|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.||Conformably overlies Bathampton Metamorphics. Is conformably overlain by Monteagle Quartzite and Hurleys Metamorphics.|Green to grey, fine-grained quartz-mica schist grading to phyllite.|23-JUN-15
23942|Rolfe Creek Schist|68482|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Anakie Province.||Of the Anakie Metamorphic Group.||Conformably overlain by the Monteagle Quartzite. Conformably underlain by the Bathampton Metamorphics.|Green to grey, fine-grained quartz-mica schist grading to phyllite.|
23942|Rolfe Creek Schist|68731|6|Mentioned|p120 Fig 3.6, p121, p122|Early Cambrian|Neoproterozoic|< 1km thick. Age constrained by the parent Anakie Metamorphic Group.||Of the Anakie Metamorphic Group.||Underlain by the Bathampton Metamorphics. Overlain by the Monteagle Quartzite.||
23942|Rolfe Creek Schist|68900|5|Briefly described|p6|||Drummond Basin.||||Overlies the Bathampton Metamorphics. Overlain by the Monteagle Quartzite.|Fine-grained mica schist grading to phyllite.|
23942|Rolfe Creek Schist|70749|6|Mentioned|p43|Cambrian|Neoproterozoic|Anakie Province.||Anakie Metamorphic Group.||||
23942|Rolfe Creek Schist|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Anakie Province, Thomson Orogen.||||||
23943|Rollingstone Granite|23422|5|Briefly described|p181, p217 Table 6.11|Carboniferous|Carboniferous|Of Oweenee Supersuite.||||||
23943|Rollingstone Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23943|Rollingstone Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 132. I-Type.||||||
23943|Rollingstone Granite|23617|4|Described|p18 Table 2|||Intrudes Paluma Rhyolite. Also see p24. Of Oweenee Supersuite of Kennedy Province.||||||
23943|Rollingstone Granite|23618|5|Briefly described|map legend||Carboniferous|||||||
23943|Rollingstone Granite|23893|5|Briefly described|p19|Early Carboniferous|Early Carboniferous|Geological Province: Oweenee Batholith.||||||
23943|Rollingstone Granite|42689|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
23943|Rollingstone Granite|43095|2|Defined|p59|Early Carboniferous||Age is not certain.||||||
23943|Rollingstone Granite|43106|5|Briefly described|p27|||||||||
23943|Rollingstone Granite|43259|4|Described|Appendix 1,p24.|Permian|Carboniferous|Carboniferous to (Permian?)||||||
23943|Rollingstone Granite|43589|2|Defined|p23||Early Carboniferous|Probably Early Carboniferous but could be as young as Early Permian? Intrudes Paluma Rhyolite and Clemant Microgranite.||||||23-APR-08
23943|Rollingstone Granite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.|||||Mottled cream and pink, fine to medium-grained, slightly to abundantly porphyritic biotite granite.|
23943|Rollingstone Granite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.|||||Mottled cream and pink, fine to medium-grained, slightly to abundantly porphyritic biotite granite.|
23943|Rollingstone Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
23944|Rollston Range Formation|22621|5|Briefly described|p204|Ordovician|Cambrian|Part of Seventy Mile Range Group.||||||10-FEB-09
23944|Rollston Range Formation|22847|5|Briefly described|p 7|||Seventy Mile Range Group||||||
23944|Rollston Range Formation|23278|5|Briefly described|Fig1p81|Ordovician|Cambrian|||||||
23944|Rollston Range Formation|23318|5|Briefly described|p392 Fig.1|Early Ordovician|Early Ordovician|Of the Seventy Mile Range Group.  Sandstone, siltstone and mudstone.  Contains Bedigonian-Chewtonian fossils.||||||10-FEB-09
23944|Rollston Range Formation|23422|4|Described|p170, p206 Table 6.3|Middle Ordovician|Cambrian|Of Seventy Mile Range Group. Underlain by Trooper Creek Formation.||||||10-FEB-09
23944|Rollston Range Formation|23430|5|Briefly described|p469|||Of Seventy Mile Creek Group.||||||
23944|Rollston Range Formation|23504|5|Briefly described|Map Legend|Ordovician|Cambrian|Oof Seventy Mile Range Group.||||||10-FEB-09
23944|Rollston Range Formation|23505|5|Briefly described|Map legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||10-FEB-09
23944|Rollston Range Formation|23764|5|Briefly described|p340|Ordovician|Cambrian|||||||
23944|Rollston Range Formation|23852|5|Briefly described|p816|Ordovician|Cambrian|Of Seventy Mile Range Group. Underlain by Trooper Creek Formation.||||||10-FEB-09
23944|Rollston Range Formation|23940|5|Briefly described|p917 Fig. 3|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group.  Formation is Fm. in text.  Geological Province:  Mount Windsor subprovince.||||||
23944|Rollston Range Formation|23950|5|Briefly described|p1134 Fig.1|Ordovician|Ordovician|Of the Seventy Mile Range Group||||||
23944|Rollston Range Formation|23952|4|Described|p1176 Fig.1|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Conformably overlies the Trooper Creek Formation. Geological Province: Mount Windsor subprovince||||||
23944|Rollston Range Formation|23953|5|Briefly described|p1202 Fig. 1|Ordovician|Cambrian|Conformably overlies the Trooper Creek Formation. Maximum Thickness: 1km. Geological Province: Mount Windsor subprovince||||||
23944|Rollston Range Formation|23954|5|Briefly described|p1228|Ordovician|Ordovician|||||||
23944|Rollston Range Formation|23988|5|Briefly described|p19 Fig.10|Early Ordovician|Early Ordovician|Of Seventy Mile Range Group.||||||
23944|Rollston Range Formation|24035|5|Briefly described|p3 Fig. 1, p6 Fig. 3|Early Ordovician|Early Ordovician|Of Seventy Mile Range Group. Siltstone, shale, and interbedded andesite.||||||
23944|Rollston Range Formation|24424|5|Briefly described|p524|Early Ordovician|Late Cambrian|Of 70 Mile Group. Geological Province: Lolworth-Ravenswood Province.||||||
23944|Rollston Range Formation|37765|5|Briefly described|p9|||||||||
23944|Rollston Range Formation|38658|6|Mentioned|p152|||||||||
23944|Rollston Range Formation|39445|6|Mentioned|p66|||||||||
23944|Rollston Range Formation|40746|3|Fully described|p351|||||||||
23944|Rollston Range Formation|42279|5|Briefly described|p27|||||||||
23944|Rollston Range Formation|42633|4|Described|p16|||||||||
23944|Rollston Range Formation|43093|5|Briefly described|p14|||Of Seventy Mile Range Group.||||||10-FEB-09
23944|Rollston Range Formation|43128|5|Briefly described|Fig.6,p476|||||||||
23944|Rollston Range Formation|43763|5|Briefly described|p742|Bendigonian|Lancefieldian|||||||
23944|Rollston Range Formation|43773|5|Briefly described|Fig.1,p765|||||||||
23944|Rollston Range Formation|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23944|Rollston Range Formation|43936|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||
23944|Rollston Range Formation|60659|5|Briefly described|p10|||Of the Seventy Mile Range Group. Overlies Trooper Creek Formation. Predominantly a sequence of of volcaniclastic siltstone and sandstone.||||||17-JUL-14
23944|Rollston Range Formation|62470|5|Briefly described|p181 Fig. 1|Ordovician|Cambrian|Uppermost unit of the Seventy Mile Range Group. Mudstone and sandstone; contains graptolites and trilobite fauna. Overlies Trooper Creek Formation. Max. thickness: ~1000m.||||||07-FEB-11
23944|Rollston Range Formation|62794|6|Mentioned|p298|Early Ordovician|Early Ordovician|Mount Windsor Subprovince, northeastern Queensland. Correlated with Horn Valley Siltstone in Amadeus Basin, NT.||||||
23944|Rollston Range Formation|64850|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Fine- to medium-grained sandstone, siltstone, shale; locally fossiliferous.||||||
23944|Rollston Range Formation|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Fine to medium-grained sandstone, siltstone and shale; locally fossiliferous.||||||
23944|Rollston Range Formation|68731|5|Briefly described|p145, p146|Early Ordovician|Neoproterozoic|Henderson (1983). Contains sporadic fossiliferous intervals with diverse graptolites and also pelagic trilobites. ~ 700-472 Ma (detailed lithology discussed.).||Of the Seventy Mile Range Group.|||Comprises laminated volcaniclastic siltstone and sandstone with rare intercalations of vitric tuff.|
23944|Rollston Range Formation|68900|4|Described|p13-p14|Chewtonian|Floian|Crops out poorly in the northern part of HARVEST HOME and PAJINGO map sheets, extending from CHARTERS TOWERS and RAVENSWOOD, where it was named by Henderson (1986). Generally elevated topography. Enriched in K relatively according to airborne radiometric images. Deposited in a sub-aqueous deep water environment. Ages derived from fossil assemblage.||Seventy Mile Range Group||Overlies the Trooper Creek Formation. Unconformably overlain by the Pallamana Sandstone.|Volcaniclastic siltstone and sandstone.|
75603|Roma Peak Granite|69594|5|Briefly described|p567 Fig.7.39, p569 Fig.7.43, p570|Early Cretaceous|Early Cretaceous|See also p571 Fig.7.47. Bowen-Mackay region. Geochemistry plots and discussion.||||Intrudes Hecate Granite.|Fine-grained leucocratic biotite monzogranite, with traces of allanite and titanite.|
27055|Ropewalk Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Forsayth Supersuite. Geological Province: Georgetown Region.||||||28-MAY-15
27055|Ropewalk Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 815. S-Type.||||||
27055|Ropewalk Granite|24197|5|Briefly described|p17, p77|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Metasedimentary xenoliths common. Age: ~1550Ma. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince). See also p79 Tb. 9.1.||||||07-FEB-11
27055|Ropewalk Granite|36216|6|Mentioned|p208|||||||||
27055|Ropewalk Granite|36937|6|Mentioned|p229|||||||||
27055|Ropewalk Granite|37570|4|Described|p119|||||||||
27055|Ropewalk Granite|39687|6|Mentioned|p3|||||||||
27055|Ropewalk Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27055|Ropewalk Granite|41272|5|Briefly described|M 1of1 B05|||||||||
27055|Ropewalk Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
27055|Ropewalk Granite|43664|5|Briefly described|p93|||||||||
27055|Ropewalk Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
27055|Ropewalk Granite|50199|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
27055|Ropewalk Granite|50210|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Part of the Forsayth Batholith.  Age: 1550-1560Ma.||||||17-MAY-04
27055|Ropewalk Granite|50537|5|Briefly described|p1.2, 1.4, 2.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.||||||
27055|Ropewalk Granite|63866|5|Briefly described|p77|||||Forsayth Supersuite||||
27055|Ropewalk Granite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Medium-grained equigranular muscovite-biotite granite, foliated and commonly melanocratic; containing biotite-rich clots and schlieren.|
27055|Ropewalk Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Dark grey, medium-grained, mostly equigranular muscovite-biotite granite, commonly foliated and melanocratic; containing biotite-rich clots and schlieren.|
27055|Ropewalk Granite|68415|5|Briefly described|Map Legend|Calymmian|Calymmian|Forsayth Batholith. Of the Etheridge Province. Shown to occur during D2 (~ 1550-1560 Ma).|~ 1560-1550 Ma||||Medium-grained equigranular muscovite-biotite granite, foliated, commonly melanocratic, containinig biotite-rich clots and schlieren.|
27055|Ropewalk Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith. Small (0.01-1.0 km2) plutons.||Forsayth Supersuite.|||Migmatitic granite bodies; strongly foliated. Enclaves and locally abundant metasedimentary xenoliths are common.|
30890|Roscow Granite|22675|4|Described|p96|Late Carboniferous|Late Carboniferous|||||||
30890|Roscow Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 234. I-Type.||||||
30890|Roscow Granite|43391|5|Briefly described|Map legend|Permian|Carboniferous|Carboniferous and/or Permian.||||||23-JUN-04
30890|Roscow Granite|43727|5|Briefly described|Table 15,p52|||||||||
30890|Roscow Granite|60659|5|Briefly described|p18|||Composite granodiorite and granite unit.||||||07-FEB-11
30890|Roscow Granite|68900|6|Mentioned|p18|||||||Intrudes the Les Jumelles beds.||
30890|Roscow Granite|69593|5|Briefly described|p495|Permian|Late Carboniferous|Burdekin Falls Subprovince.|~297-290 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
30890|Roscow Granite|70740|5|Briefly described|p20, p73, p129|Permian|Carboniferous|Outcrop characteristics and distribution briefly discussed (p129). ||||Intrudes the Les Jumelles beds, Ukalunda Formation and the Bimurra Volcanics.|Medium-grained, hornblende-biotite granodiorite to quartz monzodiorite.|
77806|Rose Creek Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Medium to coarse-grained, slightly porphyritic biotite granite.|
83085|Rosebud Granite|73553|4|Described|p18, p32, p35-36, p43-45,|Statherian|Statherian|Mary Kathleen Domain. Argylla Igneous Province. New unit. Forms a narrow, N-trending, elongate lens up to 450 m wide, south of the Rosebud homestead on the western margin of the Greens Creek Quartz Monzonite. Described by Pearson et al., (1992, p.294) as unnamed subunit '5c' of the Wonga Granite. More leucocratic than the adjacent Greens Creek Quartz Monzonite, with scarcer and smaller phenocrysts, and a not as strongly developed foliation. A-type. Separated from Wonga Igneous Subprovince in this study based on age difference. Low magnetic susceptibilities. See also  p53, p64, p74 Tb 4.1.2, p78, p80-81, p247, p249.|1790 Ma U-Pb zircon LA-ICP-MS|||Interpreted to intrude Argylla Formation|Pale grey to pale pink, fine- to medium-grained, slightly porphyritic biotite granite, foliated, extensively (and variably) recrystallised. Rare biotite-rich aggregates and mafic inclusions. Local traces of amphibole.|03-FEB-23
25451|Rosella Plains nepheline|37386|6|Mentioned|Fig.2|||||||||
25451|Rosella Plains nepheline|38310|6|Mentioned|p237|||||||||
77838|Rosetta Creek Formation|73035|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Two informal subunits recognised with mafic to intermediate volcanics. Some polygons of this unit are uncertainly identifed.|||||Siltstone to pebbly sandstone with locally abundant plant fossils; numerous, thin rhyolitic ignimbrite sheets. Coherent basalt to andesite lava; minor high-level mafic intrusives. Volcaniclastic sst; minor intermediate pyroclastic deposits.|
70429|Rosevale Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70429|Rosevale Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Coarse-grained equigranular to porphyritic biotite syenogranite.|
70429|Rosevale Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Coarse-grained equigranular to porphyritic biotite syenogranite.|
70429|Rosevale Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Coarse-grained, equigranular to porphyritic biotite syenogranite.|
70429|Rosevale Granite|73450|6|Mentioned|p16|||||||Intruded by John Clifford Road Granite.||
41098|Ross Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41098|Ross Granite|65388|2|Defined|p274, p236 Fig. 81|Early Permian|Late Carboniferous|Intrudes the Torsdale Volcanics. Age range is poorly constrained. Tentative age assigned. Very extensively weathered, pink to brown or white (bleached), medium to coarse-grained, uneven-grained to slightly porphyritic biotite granite.||||||
41098|Ross Granite|68679|5|Briefly described|p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Late Carboniferous-early Permian age is tentative.||||Intrudes Torsdale Volcanics.|Pink to brown or white, medium- to coarse-grained, uneven-grained to slightly porphyritic biotite granite.|
80926|Rosser Creek Granite|69592|6|Mentioned|p282|Early Devonian|Early Devonian|Cape York Peninsula Batholith. S-type granites. In Siluro-Devonian Pama Igneous Association.||Kintore Supersuite.||||09-DEC-19
36354|Rosser Schist|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
36354|Rosser Schist|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
36354|Rosser Schist|69591|6|Mentioned|p71 Fig.2.69|||Yambo Inlier.||||||
36354|Rosser Schist|73083|6|Mentioned|p76|||||||||
35199|Round Top Granite|23042|5|Briefly described|p106, Fig 2|Cretaceous|Jurassic|||||||
35199|Round Top Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35199|Round Top Granite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Pale pink, medium- to coarse-grained, moderately porphyritic , leucocratic monzogranite? with granophyric texture.||||||16-MAR-06
35199|Round Top Granite|65388|3|Fully described|p417, p403 Fig. 135|Cretaceous|Cretaceous|Pale brown, medium-grained, even-grained leucogranite; moderately to extensively altered. Tentative age given. On Round Top Island, near Mackay.||||||
35368|Roxmere quartz diorite|23192|6|Mentioned|p386, 387|||||||||
81636|Ruby Creek Leucogranite|71628|4|Described|p1-7; p5: 1-2, 11; p11-11; p12: 5, 10|Middle Triassic|Middle Triassic|See also p12: 12, 17; p15: 2-3, 5, 32, 34-35, 37, 40-41, 43, 49-50, 53, 55, 57-58, 62, 65-67, 70, 72-73, 75-92, 97, 99, 101-103, 112; p16: 1, 9; p19: 6, 59, 63, 83, 88, 118-119, 131, 133, 150, 159-160, 162. Flinter (1982); previously Ruby Creek Adamellite, granite, Adamellite-Granite, Granite and Leucoadamellite. Named after a local watercourse. Widely distributed (~225 km2) throughout the Stanthorpe Complex (location and brief description of the larger masses given); also occurs as dykes, pods and irregular stocks. Exposure is variable, with flatter terrain characterised by poor sandy (quartz) soil. Cut by NNE-trending vertical joints. Lithology, mineralogy, geochemistry and mineralisation (named Sn-W-Mo deposits) are detailed. Is geochemically assigned to the Ruby Creek Suite within the Stanthorpe Supersuite. RELATED UNITS (continued): Abuts Amiens and Mount Norman Leucomonzogranites; Mount Lindesay, Severn River, Jenners and The Ram Swamp Monzogranites. Partly encloses (?is intruded by) Donnellys Castle Leucomonzogranite.|241.9 +/- 1.2 Ma (SHRIMP: Chisholm et al., 2014).|Stanthorpe Complex.||Intrudes Texas beds; Wallangarra Volcanics; Bungulla, Passchendaele, Waroo, Ballandean, Jenners, Mount Marley Monzogranites; Warroo Monzogranite Phase?. See COMMENTS for more.|Pink to white, rarely pale to medium grey, very fine- to medium-grained, weakly porphyritic (marginal) to equigranular, biotite leucomonzogranite to leucosyenogranite; abundant miarolitic enclaves. I-type.|
81636|Ruby Creek Leucogranite|72078|6|Mentioned|p4|Triassic|Triassic|Geological province: New England Orogen. U-Pb SHRIMP date for zircon derived from Chisholm et al. 2014. Together with the Stanthorpe Granite forms the Ruby Creek Sn-W district.|241.9+\-1.2 Ma (SHRIMP U-Pb)|||||14-JAN-20
82409|Ruby Creek Suite|71628|5|Briefly described|p15: 35, 49, 76, 84|Middle Triassic|Early Triassic|||Stanthorpe Supersuite.|Ruby Creek Leucogranite, Donnellys Castle Leucomonzogranite (tentative).|||
36231|Rudd Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Rudd Suite. Intrudes Sundown Granite (O'Brien's Creek Supersuite); intruded by Rattler and Sandy Tate Granites. Geological Province: Georgetown Region.||||||01-JUL-15
36231|Rudd Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36231|Rudd Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 380. I-Type.||||||
36231|Rudd Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36231|Rudd Granite|23624|4|Described|p9|Permian|Carboniferous|Formerly the Herbert River Granite. Parent: Ootann Supersuite. Intruded by the Rattler Granite.||||||01-JUL-15
36231|Rudd Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey, medium-grained, even-grained biotite monzogranite; minor biotite granodiorite.|
36231|Rudd Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey, medium-grained, even-grained biotite monzogranite; minor biotite granodiorite.|
36231|Rudd Granite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|304 +/- 4 Ma.|Ootann Supersuite.||||
37889|Rudd Suite|23291|5|Briefly described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
23948|Ruddygore Granodiorite|23423|5|Briefly described|p307 Table 7.3|||Intrudes Redcap Dacite. Almaden Supersuite.||||||
23948|Ruddygore Granodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Almaden Supersuite.||||||01-JUN-09
23948|Ruddygore Granodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~300 Ma, Rb-Sr. of Almaden Supersuite.||||||
23948|Ruddygore Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 424. I-Type.||||||
23948|Ruddygore Granodiorite|23616|5|Briefly described|Table 3 p51, p41||Carboniferous|Of Almaden Supersuite.||||||
23948|Ruddygore Granodiorite|23713|5|Briefly described|p74 Appendix 2|||Intrudes the Hodgkinson Formation, Doolan Creek Rhyolite. Of Almaden Supersuite.||||||
23948|Ruddygore Granodiorite|24485|5|Briefly described|p44, p54 Tb.8|Late Carboniferous|Late Carboniferous|Age: ~302-300Ma (Rb-Sr, biotite). Intrudes the Redcap Dacite and Doolan Creek Rhyolite. Parent: Almaden Supersuite||||||
23948|Ruddygore Granodiorite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
23948|Ruddygore Granodiorite|24487|5|Briefly described|Map legend|||||||||
23948|Ruddygore Granodiorite|42681|5|Briefly described|p21|||Variation on "Ruddygore Granodiorite".||||||
23948|Ruddygore Granodiorite|43060|5|Briefly described|p61,Table 6|||of Almaden Supersuite||||||
23948|Ruddygore Granodiorite|43083|4|Described|p253|||Of the Almaden Supersuite. Intrudes Hodgkinson Formation, Redcap Dacite and Doolan Creek and Jamtin Rhyolites; cut by Bungabilly, Election, Jacks, Long Gully and Pinchgut Granites. I-type. Lithology included.||||||31-MAR-15
23948|Ruddygore Granodiorite|43087|2|Defined|p78|Late Carboniferous||Rb-Sr biotite ages of 301 - 302 Ma||||||06-MAY-08
23948|Ruddygore Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).   Medium to dark grey, fine to medium, moderately porphyritic hornblende-biotite granodiorite.  Age: 302Ma?||||||15-JUN-06
23948|Ruddygore Granodiorite|43254|5|Briefly described|map legend||Late Carboniferous|Of Almaden Supersuite.||||||01-JUN-09
23948|Ruddygore Granodiorite|43259|4|Described|Appendix 1,p46.||Late Carboniferous|Age is 302 Ma.||||||
23948|Ruddygore Granodiorite|43625|6|Mentioned|p51|||||||||
23948|Ruddygore Granodiorite|43626|6|Mentioned|p10||Late Carboniferous|||||||
23948|Ruddygore Granodiorite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: Kennedy Province. Medium to dark grey, medium-grained, slightly to moderately porphyritic hornblende-biotite granodiorite to monzogranite; mafic enclaves common.||||||
23948|Ruddygore Granodiorite|60425|4|Described|p49 Tb.3, p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Age: ~300Ma (Rb-Sr). Intruded Redcap Dacite and Doolan Creek Rhyolite in the Featherbed Volcanic Group.Very detailed lithology included for this hornblende-biotite granodiorite (283). I-type. See also p60 Tb. 4.||||||07-FEB-11
23948|Ruddygore Granodiorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Six variants are mapped separately. Low K, Th and U radiometric responses.||Unit in Almaden Supersuite.|||Pale to pale pinkish grey, fine- to medium-grained (groundmass), porphyritic biotite and hornblende granodiorites with mafic inclusions to 10 cm diameter; similar granodiorite with prominent hornblende laths.|
23948|Ruddygore Granodiorite|69593|5|Briefly described|p487 Fig.6.10|||||Almaden Supersuite.|||Locally enclave-rich.|
30149|Rugby Coal Measures|43099|4|Described|p9|||||||||
30149|Rugby Coal Measures|70815|6|Mentioned|p3|||Bowen Basin.||||||
30149|Rugby Coal Measures|72297|5|Briefly described|p694|Permian|Permian|SW of Moranbah, Bowen Basin. Includes coal of coking rank.||||||
38871|Rule Gabbro|24488|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38871|Rule Gabbro|24489|5|Briefly described|Map Legend|Triassic|Triassic|Of Glassford Igneous Complex.||||||
38871|Rule Gabbro|24615|5|Briefly described|CD|Triassic|Triassic|[Rggu].  Grey medium-grained phitic biotite-hornblende-olivine-augite gabbro, augite dolerite.||||||
38871|Rule Gabbro|67203|5|Briefly described|p7|Late Triassic|Late Triassic|Despite slightly younger K-Ar ages (Webb and McDougall, 1968), intrusive relationships indicate that this unit (and Deception Quartz Monzonite, Lawyer Granite) is marginally older than the Robert Granite (230.2+/-3.7Ma), and therefore broadly contemporaneous with the Bobby Volcanics, Agnes Water Volcanics and other granitoids further east.||Unit in Glassford Igneous Complex.||Intrudes Bobby Volcanics.||12-NOV-15
38871|Rule Gabbro|68008|2|Defined|p140, p402-403, p405-409, p411, p634-635|Late Triassic|Late Triassic|See also p637. New name, after the Parish of Rule. A 2km-wide mass extends in an arc from Station Creek, 6km westward to Coppermine Creek, with a small outcrop 2.5km NE of Mount Robert. The type area is along the southern branch of Deception Creek, from 1km above its junction with the northern branch for a further 1km upstream. Forms extremely steep, rugged, thickly forested country; access is difficult. Geophysics described in some detail and modelled; strongly magnetic. Age from relationships.||Glassford Igneous Complex.||Intrudes Littlemore Granodiorite and Lawyer Granite. Is intruded by Robert Granite and Deception Quartz Monzonite.|Altered, grey, medium- to coarse-grained biotite-hornblende-olivine-augite gabbro. The dominant constituent, subhedral laths of plagioclase to 5mm, are locally strongly aligned. Also augite microgabbro.|
38871|Rule Gabbro|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Relatively small.||Glassford Igneous Complex.|||Grey, medium-grained, ophitic, biotite-hornblende-olivine-augite gabbro, augite dolerite.|
38871|Rule Gabbro|73450|6|Mentioned|p11, p13-14|Triassic|Triassic|||||Intruded by Roberts Granite.||
24481|Rundle Formation|24420|5|Briefly described|p9|Eocene|Eocene|Of The Narrows Group.||||||
24481|Rundle Formation|24490|5|Briefly described|Map Legend|Tertiary|Tertiary|Oil shale, claystone, minor limestone and coal.  In the Narrows Graben.||||||04-SEP-08
24481|Rundle Formation|37628|6|Mentioned|p195|||||||||
24481|Rundle Formation|37676|3|Fully described|p8|||||||||
24481|Rundle Formation|38611|6|Mentioned|p186|||||||||
24481|Rundle Formation|38658|6|Mentioned|p152|||||||||
24481|Rundle Formation|39445|6|Mentioned|p169|||||||||
24481|Rundle Formation|39493|6|Mentioned|p94|||||||||
24481|Rundle Formation|39943|6|Mentioned|Table 13A|||||||||
24481|Rundle Formation|40116|4|Described|p25|||||||||
24481|Rundle Formation|41179|6|Mentioned|Fig.4|||||||||
24481|Rundle Formation|41273|5|Briefly described|p207|||||||||
24481|Rundle Formation|41927|4|Described|p64|||||||||
24481|Rundle Formation|42021|6|Mentioned|p327|||||||||
24481|Rundle Formation|50207|5|Briefly described|Map Legend|Tertiary|Tertiary|Of the The Narrows Group.||||||
24481|Rundle Formation|68008|3|Fully described|p271-273 |Eocene|Eocene|Henstridge and Missen (1982), who subdivided The Narrows Beds of Kirkegaard et al. (1970). The type section is a composite section, based on core from two boreholes: GSQ Rockhampton 2 and Southern Pacific Petroleum's RD66. Contains abundant fossil ostracods, gastropods, turtle shells, and fish and reptile fragments and coprolites.||The Narrows Group.||Overlies Worthington formation. Is overlain by Curlew Formation.|Contains at least eight oil shale seams (locally pyrite bearing), interbedded with mudstone and minor sandstone, dolomite and lignite.|
24481|Rundle Formation|69599|5|Briefly described|p589|Eocene|Eocene|Narrows Graben. Has seven Members. Has dolerite intrusions in lower parts, up to the Brick Kiln seam. Contains distinctive and diagnostic mid-Eocene microflora; also crocodiles, turtles, fish and rarer terrestrial fauna; abundant molluscs and ostracods.|||||Argillaceous sediments and oil shales.|
24481|Rundle Formation|71092|5|Briefly described|p232-234, p237|Eocene|Eocene|The Narrows Graben, SE Queensland. Lagoonal mud-flat deposits; has abundant microbial- and terrestrial and aquatic plant-derived carbonaceous matter. Fossil flora and fauna listed; vertebrates (mainly crocodiles, turtles and fish) described. Middle-late Eocene; oldest evidence of meiolaniid turtles in Australia.|||Monte Christo, Teningie Creek, Ramsay Crossing, Brick Kiln, Humpy Creek, Munduran Creek, Telegraph Creek, Kerosene Creek, Members.|Overlies Worthington Formation. Is overlain by Curlew Formation.||
24481|Rundle Formation|72297|5|Briefly described|p752-753, p755|||Up to 600m thick; most of the oil shale is in the upper 400m. Freshwater lake deposits; algae provide the source of the kerogen. Hosts the Stuart and Rundle oil shale deposits: geological map and cross-section; table of estimated resources.|||Kerosene Creek, Telegraph Creek, Munduran Creek, Humpy Creek, Brick Kiln, Ramsay Crossing, Teningie Creek, Members.||Claystone, oil shale.|
27228|Running River Metamorphics|22533|6|Mentioned|p47||Proterozoic|||||||
27228|Running River Metamorphics|22630|5|Briefly described|p 6|||||||||
27228|Running River Metamorphics|22844|6|Mentioned|p6,31,37|||||||||
27228|Running River Metamorphics|22847|5|Briefly described|p 7|||||||||
27228|Running River Metamorphics|23049|6|Mentioned|p6 Fig.3|||||||||
27228|Running River Metamorphics|23422|4|Described|p168, p206 Table 6.3|Cambrian|Neoproterozoic|Geological Province: Cape River Province.||||||
27228|Running River Metamorphics|23430|5|Briefly described|p459-462|||Cape River Province.||||||07-JUL-15
27228|Running River Metamorphics|23431|5|Briefly described|p537|||Cape River Province.||||||
27228|Running River Metamorphics|23509|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|||||||
27228|Running River Metamorphics|23617|3|Fully described|p7|Cambrian|Neoproterozoic|Also see Table 1 p12. Intruded by Falls Creek Tonalite and Kallanda Granite. Cape River Province.||||||
27228|Running River Metamorphics|23618|5|Briefly described|map legend|Cambrian|Neoproterozoic|||||||
27228|Running River Metamorphics|23893|5|Briefly described|p10|||Geological Province: Cape River Province.||||||
27228|Running River Metamorphics|24577|5|Briefly described|p752 Fig. 1|Cambrian|Proterozoic|Unconformably overlain by the Wilkie Gray Group. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
27228|Running River Metamorphics|24612|5|Briefly described|p9|||Geological Province: Burdekin Basin.||||||06-APR-05
27228|Running River Metamorphics|24613|5|Briefly described|p6 Fig. 3, p92-94|Early Devonian|Precambrian|Unconformably overlain by Ewan Formation, which is partly faulted against both Perry Creek Formation and this unit. Underlies Burdekin Basin in the Ewan area.||||||07-FEB-11
27228|Running River Metamorphics|30914|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
27228|Running River Metamorphics|31822|6|Mentioned|p71|||||||||
27228|Running River Metamorphics|31832|6|Mentioned|Table 6|||||||||
27228|Running River Metamorphics|31999|6|Mentioned|p127|||Table 11||||||
27228|Running River Metamorphics|32169|6|Mentioned|Table 2|||Precambrian||||||
27228|Running River Metamorphics|32553|4|Described|p54|||||||||
27228|Running River Metamorphics|35154|6|Mentioned|Fig.3|||||||||
27228|Running River Metamorphics|36472|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27228|Running River Metamorphics|37565|6|Mentioned|p4|||||||||
27228|Running River Metamorphics|37570|5|Briefly described|p123|||||||||
27228|Running River Metamorphics|37575|6|Mentioned|p182|||||||||
27228|Running River Metamorphics|39445|6|Mentioned|Fig. 6|||See P66, Table 4||||||
27228|Running River Metamorphics|39686|6|Mentioned|p69|||||||||
27228|Running River Metamorphics|39689|6|Mentioned|p49|||See also P61||||||
27228|Running River Metamorphics|39735|6|Mentioned|p16|||||||||
27228|Running River Metamorphics|40787|5|Briefly described|p321|||Mention Fig.2||||||
27228|Running River Metamorphics|40961|6|Mentioned|p239|||||||||
27228|Running River Metamorphics|41260|6|Mentioned|p125|||||||||
27228|Running River Metamorphics|41668|5|Briefly described|p6|||Also Fig.2.2||||||
27228|Running River Metamorphics|41735|6|Mentioned|p284|||||||||
27228|Running River Metamorphics|41774|6|Mentioned|p31|||||||||
27228|Running River Metamorphics|41916|4|Described|p25|||||||||
27228|Running River Metamorphics|42295|5|Briefly described|Fig.2 P5|||||||||
27228|Running River Metamorphics|42407|3|Fully described|p23|||||||||
27228|Running River Metamorphics|42474|4|Described|p28|||||||||
27228|Running River Metamorphics|42689|5|Briefly described|map legend|Early Paleozoic|Proterozoic|||||||07-NOV-08
27228|Running River Metamorphics|42690|5|Briefly described|map legend|Early Paleozoic|Paleoproterozoic|Early to Middle Proterozoic and/or Early Palaeozoic||||||07-NOV-08
27228|Running River Metamorphics|42692|5|Briefly described|map legend|Proterozoic||||||||
27228|Running River Metamorphics|42933|5|Briefly described|Fig. 73|||||||||
27228|Running River Metamorphics|43093|5|Briefly described|p11||Proterozoic|see also Fig.1.||||||
27228|Running River Metamorphics|43095|5|Briefly described|Plate 2.|||||||||
27228|Running River Metamorphics|43103|5|Briefly described|p17, Fig.6.|||||||||
27228|Running River Metamorphics|43120|5|Briefly described|p366|||||||||
27228|Running River Metamorphics|43213|5|Briefly described|p61|||Possible correlative of Anakie Metamorphic Group.|||||Metapelites, quartz-rich metapsammites and amphibolites with tholeiitic and alkaline basalt affinities.|
27228|Running River Metamorphics|43480|6|Mentioned|49||Devonian|||||||
27228|Running River Metamorphics|43589|6|Mentioned|p23||Proterozoic|Intruded by Coane Range Granite Complex.||||||23-APR-08
27228|Running River Metamorphics|43926|2|Defined|Tb.2,opp.p10,map,|||Formerly included in "Ewan Metamorphics" in Silurian. Now regarded as Precambrian. p10,19-20.||||||23-APR-08
27228|Running River Metamorphics|44060|14|Not recorded|Map Legend||Precambrian|||||||
27228|Running River Metamorphics|44061|4|Described|Table 1||Precambrian|||||||
27228|Running River Metamorphics|44359|14|Not recorded|Map Legend||Precambrian|||||||
27228|Running River Metamorphics|45151|6|Mentioned|p4|||See also P37.||||||
27228|Running River Metamorphics|48904|2|Defined|p7|Precambrian|Precambrian|||||||
27228|Running River Metamorphics|61211|5|Briefly described|p262 Fig. 1a|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27228|Running River Metamorphics|62074|5|Briefly described|p1|Early Cambrian|Neoproterozoic|Basement in Lolworth-Ravenswood Block. Multiply deformed; underwent high T/low P metamorphism in early to middle Ordovician.||||||
27228|Running River Metamorphics|62075|6|Mentioned|p9 Fig.2|Early Cambrian|Neoproterozoic|||||||
27228|Running River Metamorphics|63154|5|Briefly described|p285 Fig. 5|Cambrian|Early Cambrian|Geological province: Charters Towers Province.||||||11-APR-07
27228|Running River Metamorphics|67455|6|Mentioned|p574 Fig.1.|||Charters Towers Province.||||||
27228|Running River Metamorphics|68350|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.|||||Biotite gneiss, migmatite and amphibolite; laminated (para?) and massive (ortho) amphibolite; local relict pillow structures.|
27228|Running River Metamorphics|68351|5|Briefly described|Map legend.|Early Paleozoic|Neoproterozoic|Cape River Province.|||||Biotite gneiss, migmatite and amphibolite; laminated (para?) and massive (ortho) amphibolite; local relict pillow structures.|
27228|Running River Metamorphics|68419|5|Briefly described|Map Legend|Ordovician|Neoproterozoic|Of the Cape River Province. Minimum age shown as possibly Ordovician.|||||Bitotite gneiss, migmatite and amphibolite.|
27228|Running River Metamorphics|68420|5|Briefly described|Map Legend|Paleozoic|Neoproterozoic|Of the Cape River Province. Minimum age shown as possibly Ordovician.|||||Bitotite gneiss, migmatite and amphibolite.|
27228|Running River Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Charters Towers Province. This unit, as well as Argentine and Charters Towers Metamorphics, are all mapped under the symbol, -P-Cr.||||||
27228|Running River Metamorphics|68731|6|Mentioned|p115, p136, p145, p151, p183, p187|Cambrian||Charters Towers Province. (Wyatt et al. 1970; Withnall and McLennan 1991; Hutton et al. 1997).||||Unconformably overlain by the Ewan Formation.|Comprises biotite gneiss, migmatite, amphibolite, mica schist and quartzite.|
27228|Running River Metamorphics|68822|6|Mentioned|p323|||||||||
27228|Running River Metamorphics|69592|6|Mentioned|p271|||||||Structurally intercalated with Perry Creek Formation.||
27228|Running River Metamorphics|70207|6|Mentioned|p20|Paleozoic|Neoproterozoic|Clarke River and/or Cairns region.||||||
27228|Running River Metamorphics|70749|5|Briefly described|p42-43|Cambrian|Neoproterozoic|Charters Towers Province. Characterised by abundant 1300-900 Ma (late Mesoproterozoic = Grenvillian) aged detrital zircons, and maximum depositional age of ~580 Ma or older. Zircons sourced from Musgrave Province.||||||
27228|Running River Metamorphics|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Charters Towers Province, Thomson Orogen. ||||||
27228|Running River Metamorphics|73425|5|Briefly described|p1-5, 9-10, 13-16, 18-19|Neoproterozoic|Neoproterozoic|Withnall and McLennan (1991). Charters Towers Province, northeast Thomson Orogen. The MDA for the quartzite component is 470 +/- 2 Ma. Migmatite melting was dated at 434 +/- 3 Ma. With Falls Creek Tonalite, this unit is consistent with a continental magmatic arc setting. Five deformation events are described. Geochemistry detailed.|472 +/- 2 Ma (gneiss protoliths).|||Is intruded by Falls Creek Tonalite.|Greenschist to amphibolite facies metamorphic succession of mica gneisses (calc-alkaline, S-type granite protoliths), amphibolite (oceanic island basalt affinity), migmatites (I-type) and quartzite.|
27228|Running River Metamorphics|73600|6|Mentioned|p202|||||||||
36708|Rush Creek Granodiorite|23608|3|Fully described|p53, Fig 2 p49, Fig1 p50||Triassic|Previously named Station Creek Quartz monzodiorite. 231-232 Ma. Most southerly pluton in Station Creek Complex. I-Type granite. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36708|Rush Creek Granodiorite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
36708|Rush Creek Granodiorite|68679|5|Briefly described|p327-329, p411|Late Triassic|Late Triassic|Tang and Gust (2000), who gave this name to the former Station Creek Quartz Monzonite. Northern New England Orogen.|232 +/- 0.3 Ma (Ar-Ar biotite: Tang, 2004).|||Intrudes Widgee and Gobongo Metamorphics and Mount Mia Serpentinite.|Biotite-hornblende quartz monzonite; biotite granite. Reversely-zoned pluton with granite rim and granodiorite centre; monzonite stock in core may be unrelated.|
80904|Rutland Plains Granite|69593|5|Briefly described|p512|||Jardine Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|345 +/- 6 Ma.||||I-type.|
36418|Ryeburn Quartz Diorite|23617|3|Fully described|Table 2 p18|||Also see p30. Intrudes Poison Creek Granite and Mount Grey Granite. Kennedy Province.||||||
36418|Ryeburn Quartz Diorite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36418|Ryeburn Quartz Diorite|69593|5|Briefly described|p491, p495|Permian|Late Carboniferous|Bultitude et al. (1997). Ingham region. A relatively mafic unit, similar to mafic members of the Almaden Supersuite.||||||
68988|Sabina Point Schist|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Broome Head, Duckpond Road and Gaythorn Metamorphics, The Shacks Mylonite, Townshend Formation, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
68988|Sabina Point Schist|68679|6|Mentioned|p312-313, p347|Carboniferous|Late Devonian|Northern New England Orogen.||||||
68988|Sabina Point Schist|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
26129|Saddington Tonalite|23032|5|Briefly described|p21,24|||||||||
26129|Saddington Tonalite|23424|5|Briefly described|Table 8.1 p332.||Ordovician|Intrudes Judea Fm, Gray Creek Complex and Donaldsons Well Volcanic Member. Age: similar to Netherwood tonalite. I-Type. Graveyard Creek Subprovince.||||||
26129|Saddington Tonalite|23431|5|Briefly described|p540|||I-type||||||
26129|Saddington Tonalite|23513|5|Briefly described|Map legend||Ordovician|Palaeocoiz Intrusive 76. I-Type.||||||
26129|Saddington Tonalite|41260|5|Briefly described|p35|||Reserved as Saddington Quartz Diorite||||||
26129|Saddington Tonalite|41675|6|Mentioned|Fig.3|||||||||
26129|Saddington Tonalite|41679|6|Mentioned|Fig.2|||||||||
26129|Saddington Tonalite|41719|2|Defined|p215|Early Silurian|Ordovician|||||||
26129|Saddington Tonalite|41739|6|Mentioned|Fig.2|||||||||
26129|Saddington Tonalite|41740|6|Mentioned|p222|||||||||
26129|Saddington Tonalite|42054|6|Mentioned|p273|||||||||
26129|Saddington Tonalite|42279|6|Mentioned|Fig.2 P18|||||||||
26129|Saddington Tonalite|42692|5|Briefly described|map legend|Ordovician||||||||
26129|Saddington Tonalite|42693|5|Briefly described|map legend|Ordovician||||||||
26129|Saddington Tonalite|42933|3|Fully described|p54|||||||||
26129|Saddington Tonalite|43259|4|Described|Appendix 1,p20.||Ordovician|Ordovician?||||||
26129|Saddington Tonalite|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
26129|Saddington Tonalite|43480|6|Mentioned|26|||||||||
26129|Saddington Tonalite|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Broken River Province/Graveyard Creek Subprovince. Presented informallly as Saddington tonalite.||||||11-APR-07
26129|Saddington Tonalite|67455|6|Mentioned|p576. |||Graveyard Creek Subprovince, Broken River Province. Related to Donaldsons Well Volcanics.||||||
26129|Saddington Tonalite|67848|5|Briefly described|p3 Fig.2, p4, p5 Fig.3, p15 Fig.12.|Ordovician|Ordovician|Part of basement to Camel Creek Subprovince. Plutonic phases of an incipient arc assemblage.||||Intrudes Gray Creek Complex.|Diorite to tonalite.|
26129|Saddington Tonalite|68336|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||||Biotite-hornblende tonalite and quartz diorite.|
26129|Saddington Tonalite|68341|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||||Biotite-hornblende tonalite and quartz diorite.|
26129|Saddington Tonalite|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Broken River Province. This unit is mapped with the Netherwood Tonalite under the same symbol, Ogr.||||||
26129|Saddington Tonalite|69030|5|Briefly described|p6|Ordovician|Ordovician|Graveyard Creek Subprovince (Broken River Province).|487.8 +/- 2.7 Ma (SHRIMP).|||Intrudes Judea Formation.||
26129|Saddington Tonalite|69592|5|Briefly described|p251 Fig.4.35, p252-256, p258, p297|Early Ordovician|Early Ordovician|Withnall (1993). Broken River Province. An extensive unit, irregularly distributed. Geochemical plots. This c.488 Ma age is older than the overlying turbidite succession in the Judea Formation which has been dated by a graptolite occurrence.|487.8 +/- 2.7 Ma (SHRIMP U-Pb: Magee unpub. data).|||Intrudes Donaldsons Well Volcanic Member and Gray Creek Complex.|Fine- to medium-grained biotite-hornblende tonalite, diorite, quartz diorite and gabbro; multiple intrusive phases, some weakly foliated.|
26129|Saddington Tonalite|71592|5|Briefly described|Appendix A.|||Thomson Orogen.|488+/-2.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
36194|Saddle Hill Granite|23512|5|Briefly described|Map Legend||Early Permian|||||||
25747|Sagittarius Sandstone|22973|5|Briefly described|p11 Fig.2 (h)|Early Triassic|Early Triassic|Lower Rewan Group||||||
25747|Sagittarius Sandstone|23161|6|Mentioned|p33|Triassic|Late Permian|||||||
25747|Sagittarius Sandstone|24093|4|Described|p177|Early Triassic|Early Triassic|Of the Rewan Group.  Age: <251Ma.  Geological Province: Bowen Basin.  See also p176 Fig. 2.||||||
25747|Sagittarius Sandstone|31079|6|Mentioned|p17|||||||||
25747|Sagittarius Sandstone|31305|6|Mentioned|p571|||||||||
25747|Sagittarius Sandstone|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
25747|Sagittarius Sandstone|35873|6|Mentioned|Fig.9|||||||||
25747|Sagittarius Sandstone|35913|6|Mentioned|p36|||||||||
25747|Sagittarius Sandstone|36103|6|Mentioned|Table 4|||||||||
25747|Sagittarius Sandstone|36121|6|Mentioned|p25|||||||||
25747|Sagittarius Sandstone|36243|6|Mentioned|Table 3C|||||||||
25747|Sagittarius Sandstone|37612|6|Mentioned|Fig.3|||See also p284.||||||23-SEP-18
25747|Sagittarius Sandstone|38312|4|Described|p463|||||||||
25747|Sagittarius Sandstone|38518|6|Mentioned|Fig.3|||||||||
25747|Sagittarius Sandstone|38955|4|Described|p315|||||||||
25747|Sagittarius Sandstone|39212|4|Described|p14|||||||||
25747|Sagittarius Sandstone|39412|6|Mentioned|p24|||||||||
25747|Sagittarius Sandstone|39445|5|Briefly described|Table 9|||||||||
25747|Sagittarius Sandstone|39491|6|Mentioned|p24|||||||||
25747|Sagittarius Sandstone|39611|6|Mentioned|Fig.2|||||||||
25747|Sagittarius Sandstone|39943|6|Mentioned|Table 5A|||||||||
25747|Sagittarius Sandstone|42254|6|Mentioned|Fig.2 P223|||||||||
25747|Sagittarius Sandstone|42257|5|Briefly described|Table 1 P263|||||||||
25747|Sagittarius Sandstone|42911|5|Briefly described|p11|||Of Rewan Group.||||||27-MAY-08
25747|Sagittarius Sandstone|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
25747|Sagittarius Sandstone|43000|5|Briefly described|Fig.5 p112|||||||||
25747|Sagittarius Sandstone|43185|5|Briefly described|11||Triassic|||||||
25747|Sagittarius Sandstone|43714|6|Mentioned|p19|||||||||
25747|Sagittarius Sandstone|45095|1|Redefined|p23|Triassic|Triassic|||||||
25747|Sagittarius Sandstone|45110|6|Mentioned|Table 13|||||||||
25747|Sagittarius Sandstone|62921|5|Briefly described|p878 Fig.2, p881|Early Triassic|Changhsingian|Jensen (1975). SW Bowen Basin. Its base lies just above the youngest (Permian) coal.||Unit in Rewan Group.||Unconformably overlies Bandanna Formation. Is overlain conformably by Arcadia Formation.||
25747|Sagittarius Sandstone|64099|5|Briefly described|p373, p374|||Of Rewan Group. Overlies Rangal Coal Measures. P-T boundary placed at/near base. Geol Prov: Bowen Basin.||||||
25747|Sagittarius Sandstone|64856|4|Described|p68-69||Late Permian|Jensen (1975). At or near base of Rewan Group. Is overlain by Arcadia Formation. Lithic sandstone interbedded with mudstones and siltstones with scattered carbonaceous plant material. Maximum age of latest Permian.| | ||||29-NOV-17
25747|Sagittarius Sandstone|64857|5|Briefly described|p124-126|Triassic|Triassic|Fine to very coarse grained lithic sandstones interbedded with mudstones and siltstones, contained within the lower part of the Rewan Group.||||||
25747|Sagittarius Sandstone|65115|5|Briefly described|p420, Fig 14 p421|Early Triassic|Permian|Lowest unit of the Rewan Group. Fine to medium-grained sandstone and mudstone & minor coarse-grained sandstone. Locally includes the Brumby Sandstone Member at top.||||||
25747|Sagittarius Sandstone|68202|6|Mentioned|p176|Early Triassic|Early Triassic|Bowen Basin.||||||
25747|Sagittarius Sandstone|68576|5|Briefly described|Q_4: p20|||Bowen Basin.||Rewan Group.||Is overlain by Arcadia Formation.|Light green-grey, calcareous, fine- to medium-grained, rarely very coarse-grained, lithic sandstones locally with numerous shale or siltstone clasts, interbedded with green to brown mudstones and siltstones with scattered carbonaceous plant material.|
25747|Sagittarius Sandstone|68679|5|Briefly described|p377, p383|Triassic|Triassic|Jensen (1975). Bowen Basin. 300-400m thick. Meandering fluvial deposits.||||Is overlain by Arcadia Formation.|Fine- to medium-grained lithic sandstone interbedded with green to brown mudstone and siltstone; conglomerate present on eastern Basin margin.|
25747|Sagittarius Sandstone|68731|6|Mentioned|p200|||||||||
25747|Sagittarius Sandstone|71710|6|Mentioned|p386|||Bowen Basin.||||||
25747|Sagittarius Sandstone|73304|6|Mentioned|p76, p78|Induan|Changhsingian|Bowen Basin. Includes the Permian-Triassic boundary (GSSP level).||Rewan Group||||
41588|Sailor Jack Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Grey, pinkish grey, or pale pink to pink, fine- to medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite to clinopyroxene-biotite-hornblende granodiorite; locally granophyric; high magnetic response.||||||31-AUG-21
41588|Sailor Jack Granite|63748|3|Fully described|p36, p85-86 Appdx. 1|Early Triassic|Late Permian|In the Sailor Jack Suite. Intrudes Texas beds and Wallangarra Volcanics. Grey, pinkish grey or pale pink to pink, fine- to medium-grained, moderately to highly porphyritic. Contains widespread pink K-feldspar and accessory titanite. See also p27 Fig. 27.||||||07-FEB-11
41588|Sailor Jack Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Dormans Flat and Stanthorpe Granites, are all mapped under the symbol, Rgn.||||||
41588|Sailor Jack Granite|68679|5|Briefly described|p453, p455, p457-459|Early Triassic|Permian|Northern New England Batholith. ~30 km2. Geochemistry described. Is similar chemically, but not mineralogically or texturally, to the Dormans Flat Granite. Photographs, geochemical plot.||Sailor Jack Suite.||Intrudes the Wallangarra Volcanics and Texas beds.|Grey to pink, fine- to medium-grained, porphyritic; cpx-biotite-hornblende granodiorite (~20% mafics) to hornblende-biotite monzogranite (~5% mafics); granophyric intergrowths locally. Strongly oxidised-reduced, moderately evolved, high-K, I-type.|
41588|Sailor Jack Granite|68901|6|Mentioned|p8 Fig. iii|Early Triassic|Late Permian|||||||27-SEP-18
41588|Sailor Jack Granite|69639|4|Described|p1, p5, p8, p44-p50, p220, p241|Lopingian|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. Distinguishiable mineralogically and texturally but not chemically from the Ballandean Granite.|253.1 +/- 1.5 Ma (SHRIMP U-Pb)|Sailor Jack Suite||Intrudes the Texas Beds and Wallangara Volcanics (Wandsworth Volcanic Group).|Equigranular to inequigranular, medium- to coarse-grained granite.|
41588|Sailor Jack Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|253+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
41588|Sailor Jack Granite|71628|6|Mentioned|p12: 1, 12|||Donchak et al. (2007). Now Sailor Jack Monzogranite.||||||
82413|Sailor Jack Monzogranite|71628|3|Fully described|p5-1; p12: 1-2, 4-5, 7, 10, 12-19|||See also p15-57; p19: 6, 8. New name. Originally mapped as part of Stanthorpe Adamellite then Stanthorpe Monzogranite; later Sailor Jack Granite (Donchak et al., 2007). Probably named after Sailor Jack homestead. Type area is near MGA 379891 6796872, on Sailor Jack Station. It is unclear whether granodiorite or monzogranite dominates. Crops out over 30 km2 about 13 km W of Wallangarra. Forms tors, scattered boulders and pavements. Geochemistry described.|253.1 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Sailor Jack Suite.||Intrudes Texas beds (and locally is faulted against it), Wallangarra Volcanics and Ballandean Monzogranite.|Pale pink to pale grey, fine- to medium-grained, moderately to highly porphyritic hornblende-biotite monzogranite to clinopyroxene-biotite-hornblende granodiorite; locally granophyric. I-type.|
73887|Sailor Jack Suite|63748|5|Briefly described|p36, p43|Early Triassic|Late Permian|Of the Ballandean Supersuite. Includes Sailor Jack Granite.||||||07-FEB-11
73887|Sailor Jack Suite|68679|5|Briefly described|p457-458|Early Triassic|Permian|Northern New England Batholith.||Stanthorpe Supersuite.|Dormans Flat, Sailor Jack, Granites.|||
73887|Sailor Jack Suite|69639|5|Briefly described|p44, p220|||New England Orogen.||Ballandean Supersuite||||
73887|Sailor Jack Suite|71628|5|Briefly described|p12: 1, 3-4, 6, 8, 10-11, 13, 15|||Donchak et al. (2007); they initially included it in their Ballandean Supersuite. Reassigned to Sailor Jack Supersuite in this study. Appears erroneously as Sailor Jack Group on p12-6.||Sailor Jack Supersuite.|Sailor Jack Granite.; Accommodation Creek, Blacksmiths Creek, Passchendaele Monzogranites.|||
82412|Sailor Jack Supersuite|71628|5|Briefly described|p1-7; p12: 1-19; p15: 33, 52-53, 65, 75|Early Triassic|Permian|See also p19: 159-160. New unit; includes intermediate granites in the Ballandean-Tenterfield-Stanthorpe area. Apparently previously included in the Bungulla Monzogranite. Geochemically most similar to Llangothlin Suite.|||Sailor Jack, Dormans Flat, Gleamwoods, Quartz Pot Creek, Strathaven Suites: Accommodation Creek, Blacksmiths Creek, Storm King, Monzogranites.||Typically grey, pinkish-grey, pale pink to pink, fine-medium grained, porphyritic granodiorite to monzogranite. K-feldspar phenocrysts range from pink to white; ferromagnesians primarily hornblende and biotite. I-type.|
36497|Saint Georges Tree Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 129.||||||
23953|Saint Giles Volcanics|23422|5|Briefly described|p181, p205 Table 6.3|Early Carboniferous|Early Carboniferous|Equivalent to Tareela Volcanics, Glenrock Group.||||||21-APR-08
23953|Saint Giles Volcanics|23430|6|Mentioned|p489|||||||||
23953|Saint Giles Volcanics|23431|5|Briefly described|p538|||||||||
23953|Saint Giles Volcanics|23509|5|Briefly described|Map Legend||Carboniferous|||||||
23953|Saint Giles Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V62. Assumed to be I-Type.||||||
23953|Saint Giles Volcanics|23893|5|Briefly described|p18|Carboniferous|Carboniferous|Geological Province: Kennedy Province.||||||
23953|Saint Giles Volcanics|24613|6|Mentioned|p113, p115 Fig. 20 |||||||||07-FEB-11
23953|Saint Giles Volcanics|42689|5|Briefly described|map legend|Carboniferous||Actually spelt St Giles Volcanics.||||||
23953|Saint Giles Volcanics|43095|2|Defined|p29|Early Carboniferous||||||||
23953|Saint Giles Volcanics|43259|4|Described|Appendix 1,p6.||Early Carboniferous|||||||
23953|Saint Giles Volcanics|43589|2|Defined|p19||Early Carboniferous|Previously included in the "Unnamed Acid Volcanics" (Cuv) of Wyatt et al (1970).  Other parts of this original unnamed unit now assigned to Tareela Volcanics and Watershed North Rhyolite.||||||23-APR-08
23953|Saint Giles Volcanics|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Kennedy Province.|||||Grey to dark grey, sparsely to moderately crystal- and clast-rich, rhyolitic to dacitic ignimbrite, lapilli tuff and minor breccia; minor flow-banded, spherulitic, moderately porhyritic rhyolite lava.|
23953|Saint Giles Volcanics|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Kennedy Province.|||||Grey to dark grey, sparsely to moderately crystal- and clast-rich, rhyolitic to dacitic ignimbrite, lapilli tuff and minor breccia; minor flow-banded, spherulitic, moderately porhyritic rhyolite lava.|
23953|Saint Giles Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
23953|Saint Giles Volcanics|69593|5|Briefly described|p495-496|Visean|Visean|Forms scattered outcrops in the Townsville region.|||||Crystal-rich to lithic-rich rhyolitic to dacitic ignimbrite; minor tuff, lava, breccia.|
22803|Saint Helena Monzogranite|23423|5|Briefly described|p315 Table 7.4||Early Permian|Lags Supersuite.||||||
22803|Saint Helena Monzogranite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Of Lags Supersuite.||||||
22803|Saint Helena Monzogranite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 435. A-Type.||||||
22803|Saint Helena Monzogranite|23616|6|Mentioned|p80|||||||||
22803|Saint Helena Monzogranite|43060|5|Briefly described|p112|||of Lags Supersuite||||||
22803|Saint Helena Monzogranite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Medium to dark grey, very strongly porphyritic garnet-augite-hypersthene-biotite microgranodiorite to microgranite, hornblende-biotite microgranodiorite to microdiorite,||||||15-JUN-06
22803|Saint Helena Monzogranite|43259|4|Described|Appendix 1,p47.||Permian|||||||
22803|Saint Helena Monzogranite|43567|5|Briefly described|Table 1,p400|||||||||
22803|Saint Helena Monzogranite|43626|6|Mentioned|p43|||||||||
22803|Saint Helena Monzogranite|60425|4|Described|p47 Tb. 3, p58 Tb. 4, p77, p276-7 App. |Early Permian|Early Permian|Of Lags Supersuite. Age: 279+/-4Ma and 280+/-4Ma. A-type. Cuts Yongala Volcanic Subgroup units. Medium to dark grey, very highly porphyritic garnet-augite-hypersthene-biotite microgranodiorite to microgranite - additional lithology included.||||||07-FEB-11
22803|Saint Helena Monzogranite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Lags Supersuite.|||Medium to dark grey, highly porphyritic (garnet-augite-hypersthene-) biotite microgranodiorite to microgranite; subordinate hornblende-biotite microgranodiorite to microdiorite.|
22803|Saint Helena Monzogranite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Lags Supersuite.|||A-type.|
27230|Saint James Volcanics|23422|5|Briefly described|p180, p205 Table 6.3|Late Carboniferous|Early Carboniferous|Of Glenrock Group.||||||
27230|Saint James Volcanics|23430|5|Briefly described|p506|||Of Glenrock Group. Burdekin Basin Province.||||||
27230|Saint James Volcanics|23431|5|Briefly described|p538|||of Glenrock Group.||||||
27230|Saint James Volcanics|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group.||||||
27230|Saint James Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V59.||||||
27230|Saint James Volcanics|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
27230|Saint James Volcanics|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin. Saint is St. in text of figure.||||||06-APR-05
27230|Saint James Volcanics|24613|2|Defined|p6 Fig. 3, p101|Early Carboniferous|Early Carboniferous|Of Wyatt et al (1970); also used Ben Lomond Volcanics (unpubl.) for part of unit.Over Keelbottom Gp; below Watershed Rhyolite.Thickness: ~1500m.Geol.prov: Burdekin Basin. Basalt, rhyolite, sst, minor chert; breccia, tuff, ignimbrite. Saint is St in Fig.3||||||07-FEB-11
27230|Saint James Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27230|Saint James Volcanics|32169|6|Mentioned|Table 2|||U.Carb.||||||
27230|Saint James Volcanics|32553|4|Described|p44|||||||||
27230|Saint James Volcanics|34408|6|Mentioned|p185|||On table||||||
27230|Saint James Volcanics|36061|4|Described|p27|||||||||
27230|Saint James Volcanics|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
27230|Saint James Volcanics|37573|6|Mentioned|p226|||See also Fig.2||||||
27230|Saint James Volcanics|37613|6|Mentioned|p249|||See also Fig.3||||||
27230|Saint James Volcanics|39445|5|Briefly described|Table 7|||Uranium in welded tuff. See also P92||||||
27230|Saint James Volcanics|39686|6|Mentioned|p73|||||||||
27230|Saint James Volcanics|41125|5|Briefly described|p54|||Mention P51 and Fig.29||||||
27230|Saint James Volcanics|41774|6|Mentioned|Table 1|||||||||
27230|Saint James Volcanics|41916|6|Mentioned|p33|||||||||
27230|Saint James Volcanics|42295|5|Briefly described|Fig.2 P5|||||||||
27230|Saint James Volcanics|42407|6|Mentioned|p22|||||||||
27230|Saint James Volcanics|42547|5|Briefly described|p76|||Actually spelt St James Volcanics.||||||
27230|Saint James Volcanics|42689|5|Briefly described|map legend|Carboniferous||Actually spelt St James Volcanics.||||||
27230|Saint James Volcanics|43095|1|Redefined|p17|Early Carboniferous||||||||
27230|Saint James Volcanics|43259|4|Described|Appendix 1,p6.||Early Carboniferous|Age Early Carboniferous?||||||
27230|Saint James Volcanics|43589|1|Redefined|p17|Early Carboniferous|Early Carboniferous|North Queensland Volcanic and Plutonic Province (NQVP).||||||23-APR-08
27230|Saint James Volcanics|44060|14|Not recorded|Map Legend|Early Permian|Late Carboniferous|||||||
27230|Saint James Volcanics|44061|4|Described|Table 3||Late Carboniferous|||||||
27230|Saint James Volcanics|45151|6|Mentioned|Table 6|||||||||
27230|Saint James Volcanics|46845|6|Mentioned|p143|||||||||
27230|Saint James Volcanics|48904|2|Defined|p40|Late Carboniferous|Late Carboniferous|||||||
27230|Saint James Volcanics|66529|5|Briefly described|p24,p25 Fig.9, |Carboniferous|Carboniferous|St. James Volcanics in text. Hosts the rich Ben Lomond uranium deposit.||Unit in Glenrock Group.||Overlies the Keelbottom Group. Is overlain unconformably by Watershed North Rhyolite.|Includes calc-alkaline volcanics.|
27230|Saint James Volcanics|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin. Subdivided into 5 unnamed units.||Of the Glenrock Group.|||Pale green, spherulitic, flow-banded rhyolite and rhyolitic tuff and breccia; dark grey aphyric amygdaloidal basaltic lava and breccia; pale pink rhyolitic breccia; rhyolitic lapilli tuff, volcaniclastic arenite, chert; aphyric to porphyritic basalt.|
27230|Saint James Volcanics|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin. Informally subdivided into 5 unnamed units.||Of the Glenrock Group.|||Pale green, sperulitic, flow-banded rhyolite and rhyolitic tuff and breccia; dark grey aphyric, amygdaloidal basaltic lava and breccia; pale pink rhyolitic breccia; rhyolitic lapilli tuff, volcaniclastic arenite, chert; aphyric to porphyritic basalt.|
27230|Saint James Volcanics|68731|5|Briefly described|p187|Pennnsylvanian|Pennnsylvanian|Adjacent to Keelbottom Creek west of Townsville and conformably succeeds the Horse Pocket Volcanics. Assigned a late Pennsylvanian age.|||||Comprises aphyric, amygdaloidal basalt and basalt breccia, rhyolitic breccia and subordinate coarse to pebbly volcaniclastic sandstone (lower); ignimbrite, aphyric, spherulitic and banded flows and lapilli tuff (upper).|
27230|Saint James Volcanics|69593|5|Briefly described|p495-496|Visean|Visean|Charters Towers region; Broken River Province.||Glenrock Group.|||Includes basaltic and andesitic lava, rhyolitic ignimbrite, tuff and pyroclastic rocks.|
35540|Saint Lawrence Suite|23162|5|Briefly described|p876|||This is collective term for all chemically discreet outlying plutons south of the Urannah Batholith. Spelt as St Lawrence Suite.||||||
35540|Saint Lawrence Suite|68679|5|Briefly described|p363|||Allen et al. (1998); one of their three Suites comprising the Carboniferous-early Permian Urannah Batholith. Geochemistry summarised.|||||I-type.|
22804|Saint Michael Member|24613|3|Fully described|p67|Tournaisian|Tournaisian|Of Hardwick Formation.||||||07-FEB-11
22804|Saint Michael Member|24614|5|Briefly described|p192, p199|Tournaisian|Tournaisian|Prominent calcareous interval within the Hardwick Formation. Calcareous sandstones, arenaceous limestones and occasionally oolitic calcarenites with shale and mudstone interbeds. Max. thickness: <820m.||||||18-JUL-14
22804|Saint Michael Member|68731|6|Mentioned|p187|Mississippian|Mississippian|Age constrained by the Hardwick Formation.||Of the Hardwick Formation.||||
24485|Saint Mungo Granite|23079|6|Mentioned|p701|||||||||
24485|Saint Mungo Granite|24197|5|Briefly described|p32, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24485|Saint Mungo Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24485|Saint Mungo Granite|37862|4|Described|p586|||||||||
24485|Saint Mungo Granite|38310|6|Mentioned|p237|||||||||
24485|Saint Mungo Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24485|Saint Mungo Granite|39445|5|Briefly described|Table 2|||||||||
24485|Saint Mungo Granite|40840|6|Mentioned|Map legend|||||||||
24485|Saint Mungo Granite|45161|5|Briefly described|p32|||See also P25||||||
24485|Saint Mungo Granite|45166|5|Briefly described|p34|||||||||
24485|Saint Mungo Granite|49009|2|Defined|p38|Proterozoic|Proterozoic|Previously mapped as part of the Kalkadoon Granite (Carter & Opik, 1963).||||||13-OCT-08
24485|Saint Mungo Granite|49041|5|Briefly described|Table 2|||||||||
24485|Saint Mungo Granite|50100|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Burstall Suite (Wonga Batholith). Geological Province: Kalkadoon-Ewen and Eastern Fold Belt Provinces.||||||13-OCT-08
24485|Saint Mungo Granite|50536|5|Briefly described|p1.1, 1.4, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||07-NOV-08
24485|Saint Mungo Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Hornblende-biotite granite.||||||
24485|Saint Mungo Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Porphyritic hornblende-biotite granite; minor porphyritic biotite granite, aplite. Weakly foliated to gneissic.|
24485|Saint Mungo Granite|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic hornblende-biotite granite (subsurface)|
24485|Saint Mungo Granite|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic hornblende-biotite granite|
24485|Saint Mungo Granite|69591|5|Briefly described|p60|||||Burstall Suite.|||Porphyritic hornblende-biotite granite; minor porphyritic biotite granite, aplite; weakly foliated to gneissic.|
24485|Saint Mungo Granite|73413|6|Mentioned|p5-6, p8-10, p21-24|Orosirian|Orosirian|[Also written as Saint Mungo granite]. New U-Pb zircon ages of 1850 +/- 6 Ma and 1790 +/- 7 Ma reported herein. A small inlier of this unit was locally mapped within intrusions of the Tick Hill Complex immediately west of Tick Hill; this inlier was reassigned as remnant Kalkadoon Supersuite (One Tree Granite[?]).|1850 +/- 6 Ma, 1790 +/- 7 Ma|Burstall Suite||Intrudes the Corella Formation and Plum Mountain Gneiss.|Includes granitic gneiss.|
24485|Saint Mungo Granite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mary Kathleen Domain.|||||Felsic intrusive.|
24485|Saint Mungo Granite|73553|4|Described|p1, p36, p47, p49-50, p53, p253-259|Statherian|Orosirian|Big Toby (?) Igneous Province. Formerly included in ~1740 Ma Burstall Suite of Budd et al., (2001). A-type. Included in the Kalkadoon Granite of Carter and Opik (1963), subsequently delineated as a discrete unit by Blake et al., (1981a, b, 1982a). Crops out in a NW to N-trending belt from west of The Monument north to the Plum Mountain Fault. Predominantly mottled pale pink-pale red on radiometric images. Very low response on aeromagnetic images. A-type characteristics. Extensively altered (Na- (Ca-) metasomatised) in places. Cut by metadolerite dykes. Recent dating of the granite means that the postulated relationships with adjacent units mapped as Argylla Formation and Corella Formation require reassessment. See also p36 Fig.3.4.4.|1798+/-6 Ma U-Pb zircon LA-ICP-MS|||Intrudes Plum Mountain Gneiss and Corella Formation, may be intruded by Birds Well Granite|Partly recrystallised, pink, highly porphyritic, fine-grained amphibole-biotite granite containing abundant phenocrysts of K-feldspar, sparse mafic inclusions and rare inclusions of microgranite.|03-FEB-23
36185|Saint Patricks Hill Granite|23423|5|Briefly described|p241|||Of O'Briens Creek Supersuite.||||||
36185|Saint Patricks Hill Granite|23507|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
36185|Saint Patricks Hill Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 254. I-Type.||||||
36193|Saint Pauls Hill Microgranite|23423|5|Briefly described|p310 table 7.4||Early Permian|I-type granite.||||||
36193|Saint Pauls Hill Microgranite|23512|5|Briefly described|Map Legend||Early Permian|||||||
36193|Saint Pauls Hill Microgranite|60425|5|Briefly described|p54 Tb. 4, p272-3 Appdx. 1|Early Permian|Early Permian|Of Saint Pauls Hill Suite (Cape Melville Supersuite). Intruded Hodgkinson Formation. I-type. Grey, fine-grained, highly porphyritic (allanite-) hornblende-biotite granite; with sparse inclusions of mainly biotite-rich metasediments.||||||07-FEB-11
36193|Saint Pauls Hill Microgranite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Saint Pauls Hill Suite.||||
75146|Saint Pauls Hill Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Cape Melville Supersuite. Contains Saint Pauls Hill Microgranite and the informally named Abbey Peak granite currently being included in Cape Melville Granite. I-type.||||||07-FEB-11
75146|Saint Pauls Hill Suite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. |||Saint Pauls Hill Microgranite, Abbey Peak granite.|||
24486|Saint Ronans Metamorphics|24419|5|Briefly described|p14, p12 Fig. 4, p15 Fig. 6|Paleoproterozoic|Paleoproterozoic|Intruded by Sybella Suite granites.  Highly deformed and metamorphosed volcanics and sediments.  Unconformably overlain by Jayah Creek and Oroopo Metabasalts. Geol.Prov: Western Fold Belt, Leichardt River Subprovince (Mount Isa Orogen)||||||07-NOV-08
24486|Saint Ronans Metamorphics|37862|4|Described|p587|||||||||
24486|Saint Ronans Metamorphics|38234|4|Described|p103|||||||||
24486|Saint Ronans Metamorphics|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24486|Saint Ronans Metamorphics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24486|Saint Ronans Metamorphics|39445|5|Briefly described|Table 2|||||||||
24486|Saint Ronans Metamorphics|40840|6|Mentioned|Map legend|||||||||
24486|Saint Ronans Metamorphics|41381|6|Mentioned|p325|||||||||
24486|Saint Ronans Metamorphics|41978|6|Mentioned|p498|||||||||
24486|Saint Ronans Metamorphics|41979|6|Mentioned|Fig.2 P512|||||||||
24486|Saint Ronans Metamorphics|43928|6|Mentioned|20,25|||||||||
24486|Saint Ronans Metamorphics|45161|4|Described|p11|||||||||
24486|Saint Ronans Metamorphics|45166|6|Mentioned|p7|||See also p10||||||02-APR-07
24486|Saint Ronans Metamorphics|49009|2|Defined|p39|Precambrian|Precambrian|Mapped as Eastern Creek Volcanics by Noakes & others (1959).||||||
24486|Saint Ronans Metamorphics|49041|5|Briefly described|Table 1|||||||||
24486|Saint Ronans Metamorphics|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Geological Province: Western Fold Belt Province.||||||
24486|Saint Ronans Metamorphics|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
24486|Saint Ronans Metamorphics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Schist, quartzite, amphibolite, felsic metavolcanics, metabasalt.||||||
24486|Saint Ronans Metamorphics|61933|5|Briefly described|p169 Fig.1, p181|||Includes coarse-grained schists. Saint is St in text.||||||02-APR-07
24486|Saint Ronans Metamorphics|61936|6|Mentioned|p193|||Includes greenschist facies schist and phyllite. Saint is St in text. ||||||
24486|Saint Ronans Metamorphics|63866|5|Briefly described|p57|Orosirian||Leichhardt River Fault Trough.|>1850 Ma|||||
24486|Saint Ronans Metamorphics|64250|5|Briefly described|p8, p9 fig 1, p11 fig 3, p19, p22|||Basement of Western Fold Belt, Mount Isa Inlier.||||||
24486|Saint Ronans Metamorphics|65387|5|Briefly described|p1, p3 Tb.1, p64-69, p82-83|||Written as St Ronans Metamorphics in text. An intrusive unit was dated at 1787 +/- 4 Ma, and an overlying volcaniclastic unit [Bucket Hole Metavolcanics] has a maximum depositional age of 1823 +/- 8 Ma.|||?Includes Bucket Hole Volcanics.||Includes felsic pegmatite intrusive.|18-SEP-18
24486|Saint Ronans Metamorphics|65396|6|Mentioned|p82, p171-172, p175, p186, p241, p438|||Lawn Hill Platform. Basement to Mount Isa Inlier.||||||
24486|Saint Ronans Metamorphics|67323|5|Briefly described|GIS attrib tbl, p7, p23, p29, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Ardmore - May Downs Domain, Mount Isa Inlier. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny. Intrusive part dated at 1787+/-4 Ma.|||||Felsic schist, metavolcanics, metabasalt, quartzite.|
24486|Saint Ronans Metamorphics|68146|5|Briefly described|p194|||Intruded by 1787 +/- 4 Ma pegmatites (Carson et al., 2008). |||||Low-grade metasediments.|
24486|Saint Ronans Metamorphics|68553|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Pre-Barramundi Orogeny basement. This unit, as well as Yaringa Metamorphics and Sulieman Gneiss, are all mapped under the symbol, -Px.||||||
24486|Saint Ronans Metamorphics|68575|6|Mentioned|p124|||Low-grade metamorphics. Intruded by pegmatites aged c.1787 Ma.||||||
24486|Saint Ronans Metamorphics|69591|5|Briefly described|p29-32, p58|Paleoproterozoic|Paleoproterozoic|One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma). Considered part of the same depositional package as the Murphy and Yaringa Metamorphics.|1787 +/- 4 Ma (Carson et al., 2008).||||Felsic schist, metavolcanics, metabasalt, quartzite.|
24486|Saint Ronans Metamorphics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1829+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Volcaniclastic rock.|
24486|Saint Ronans Metamorphics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
24486|Saint Ronans Metamorphics|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Metamorphics.|
76889|Saint-Smith Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin|||||Almost entirely quartzite and sandstone, very rare siltstone|
76889|Saint-Smith Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Pilpah and Bularnu Formations under the symbol, -Pp.||||||
76889|Saint-Smith Formation|68575|5|Briefly described|p3, p6-7, p36-p44, p125, p127, p134|||New name. Saint-Smith Range, Mount Isa Region. Comprises rocks previously mapped (Mount Isa 1:250 000 sheet) as Surprise Creek Formation. Overlain by a thick package of pebble to cobble conglomerate mapped as Torpedo Creek Quartzite. Both these units are renamed as Saint-Smith Formation and (unconformably or disconformably) overlying Bularnu Formation. Shallow marine deposits. Various age determinations discussed. Too young to belong to the Myally Supersequence. Could be part of the Prize Supersequence, but probably belong to the Bigie [actually Big] Supersequence: may be a marine equivalent of Bigie Formation. Provenance (detrital zircon populations) is similar to Bularnu Formation but significantly different from Torpedo Creek Quartzite. Whole rock Sm-Nd isotopic data and age (1736 Ma).|1736 +/- 12 Ma (maximum depositional age).|||Is overlain by Bularnu Formation unconformably or disconformably.|Low-grade psammite: fine- to medium-grained, poorly to moderately sorted quartzose sandstones.|17-JAN-17
76889|Saint-Smith Formation|69591|5|Briefly described|p29, p56|Paleoproterozoic|Paleoproterozoic|Mount Oxide Domain, Mount Isa Province. Part of the ?Prize Supersequence. Fluvial/shallow-marine deposits.|1736 +/- 12 Ma (Magee et al., in press).||||Quartzite and sandstone; very rare siltstone.|
76889|Saint-Smith Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
75650|Salitros Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, slightly porphyritic biotite monzogranite; with rare hornblende, traces of allanite and scattered mafic inclusions up to c. 15 cm across.|
75650|Salitros Granite|73037|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, slightly porphyritic biotite monzogranite; with rare hornblende, traces of allanite and scattered mafic inclusions up to c. 15 cm across.|
33930|Saltmine Creek monzogranite|22465|6|Mentioned|p935|||||||||
30354|Saltpan volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V68. I-Type.||||||
30354|Saltpan volcanics|43259|5|Briefly described|Appendix 1,p7||Carboniferous|||||||
41788|Sambo Quartz Monzonite|60475|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Pinkish-grey, medium grained augite-biotite quartz monzonite to quartz monzodiorite.||||||
41788|Sambo Quartz Monzonite|61035|4|Described|p9 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Mountain View Volcanics and unconformably overlain by Carmila beds. Age: 314+/-1.7Ma (M. Fanning, SHRIMP). Geological Province: Connors Sudprovince. Medium-grained augite-biotie quartz monzonite to quartz monzodiorite.||||||07-FEB-11
41788|Sambo Quartz Monzonite|65388|2|Defined|p358, 399, p90 Fig. 37|Late Carboniferous|Late Carboniferous|New name. Appears to intrude Mountain View Volcanics and possibly Whelan Creek Volcanics, although no contacts observed. Overlain by Carmila beds. SHRIMP zircon age 314.8+/- 3.8 Ma. Pinkish-grey, medium-grained augite-biotite quartz monzonite to quartz monzodiorite.||||||
41788|Sambo Quartz Monzonite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus,Toobier, Tooloombah Creek and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites, are all mapped under the same symbol, Cgc.||||||
41788|Sambo Quartz Monzonite|68679|6|Mentioned|p347|Carboniferous|Carboniferous|Northern New England Orogen. See also reference to [?mis-spelt] Sambo Granite (p362).||||||
41788|Sambo Quartz Monzonite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|314+/-3.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
36228|Sandy Tate Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Sandy Tate Suite. Intrudes Mount Cardwell, Sundown and Rudd Granites; intruded by Flat Rock granite. Geological Province: Georgetown Region.||||||01-JUL-15
36228|Sandy Tate Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36228|Sandy Tate Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 377. I-Type.||||||
36228|Sandy Tate Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36228|Sandy Tate Granite|23624|4|Described|p11|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||01-JUL-15
36228|Sandy Tate Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Sandy Tate Suite (Ootann Supersuite). I-type. White to pink, coarse-grained, even-grained to slightly porphyritic hornblende-biotite granite.||||||07-FEB-11
36228|Sandy Tate Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, coarse-grained, even-grained to slightly porphyritic hornblende-biotite monzogranite.|
36228|Sandy Tate Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, coarse-grained, even-grained to slightly porphyritic hornblende-biotite monzogranite.|
37892|Sandy Tate Suite|23291|5|Briefly described|p96 Tb. 3.11, p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Ootann Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
37892|Sandy Tate Suite|60425|5|Briefly described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. Contains the Sandy Tate Granite. I-type.||||||07-FEB-11
28025|Saraga Schist|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
28025|Saraga Schist|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
28025|Saraga Schist|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
28025|Saraga Schist|43596|4|Described|p11-12, , p21 Tb. 1||Proterozoic|Of Yambo Metamorphic Group.  Faulted against Annie Creek Schist in W, and against Jedda Schist in NE. Geological province: Yambo Inlier. Consists of a range of metasedimentary and meta-igneous rock types subdivided into 6 subunits, mainly schist and gneiss.||||||07-APR-15
28025|Saraga Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|Yambo Metamorphic Group||||||24-JAN-05
28025|Saraga Schist|50537|5|Briefly described|p6.1|||Of the Yambo Metamorphic Group. Geological Province: Yambo Inlier.||||||
28025|Saraga Schist|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Is intruded by the Cape York Peninsula Batholith.||Yambo Metamorphic Group.||Is intruded by Arkara Gneiss. Is faulted against Annie Creek and Jedda Schists and Pombete Gneiss.|Sillimanite-garnet two-mica schist and gneiss, quartzite, minor mafic granulite, amphibolite, abundant mylonitic granite/granodiorite.|
29331|Saucebottle Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Carboniferous|Parent: Saucebottle Suite. Intrudes Kitchener Granite; intruded by McCord (O'Brien's Creek Supersuite), Gelaro, Mount Cardwell Granites, and Martin Creek Microgranite.   Geological Province: Georgetown Region.||||||30-MAR-15
29331|Saucebottle Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
29331|Saucebottle Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29331|Saucebottle Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
29331|Saucebottle Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 321. I-Type.||||||
29331|Saucebottle Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29331|Saucebottle Granite|23624|4|Described|p14|Permian|Carboniferous|Parent: Ootann Supersuite.||||||30-MAR-15
29331|Saucebottle Granite|43083|5|Briefly described|p256|||Of Ootann Supersuite. I-type. Lithology included.||||||01-JUL-15
29331|Saucebottle Granite|43087|2|Defined|p40|Late Carboniferous||Of Ootann Supersuite. Reserved as Saucebottle Creek Adamellite.||||||
29331|Saucebottle Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|Late? Carboniferous in age.||||||
29331|Saucebottle Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
29331|Saucebottle Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, medium-grained, porphyritic biotite monzogranite, with large megacrysts of white K-feldspar; a white to pink, coarse-grained, even-grained biotite granite variant is mapped separately.|
29331|Saucebottle Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to grey, medium-grained, porphyritic biotite monzogranite, with large megacrysts of white K-feldspar; a white to pink, coarse-grained, even-grained biotite granite variant is mapped separately.|
29331|Saucebottle Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The four variants are mapped separately.||Unit in Ootann Supersuite.|||Pale grey to pinkish grey, fine-grained, moderately to highly porphyritic, (muscovite)-biotite monzogranite; coarse-grained biotite granite; biotite monzogranite; pink, fine- to medium-grained, leucocratic (muscovite)-biotite monzogranite.|
29331|Saucebottle Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|Informally subdivided into two units.||Porphyritic (hornblende-) biotite granite to granodiorite?; white to pink, coarse-grained, even-grained biotite granite.|
40136|Sawnee Gabbro|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRTgas].  Grey, medium-grained hornblende gabbro.||||||
40136|Sawnee Gabbro|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
40136|Sawnee Gabbro|68008|2|Defined|p373, p377-378|Early Triassic|Permian|New name. The type area comprises the ridges W of the Calliope River leading up to Mount Sawnee, from which the unit derives its name. Forms a continuous E-W belt 8 x 1km between the headwaters of the Don and Calliope Rivers. Has a prominent positive magnetic feature. Associated with small garnetiferous skarn deposits, some with minor base metals, in the Balaclava Formation.||Galloway Plains Igneous Complex.||Intrudes Balaclava Formation and Youlambie Conglomerate. Is possibly intruded by Rocky Point Granodiorite.|Mainly hornblende gabbro, with lesser hornblende-hypersthene-augite gabbro. Plagioclase is the dominant mineral, making up 55-65% of the rocks as subhedral laths to 4mm, locally aligned.|
40136|Sawnee Gabbro|68679|5|Briefly described|p424-425|||Yarrol Province. Forms a narrow belt ~8km long along the NW margin of the Complex. One of the earliest phases of the Complex.||Galloway Plains Igneous Complex.||Intrudes Balaclava Formation and Youlambie Conglomerate. May be intruded by Rocky Point Granodiorite.|Hornblende gabbro.|
40136|Sawnee Gabbro|72297|5|Briefly described|p728|Early Triassic|Permian|Hosts the Mount Allison garnet-magnetite skarn, 50km W of Gladstone; indicated and measured resources of 793,585 t garnet.||||||
24488|Sawpit Granodiorite|35920|2|Defined|p21|Mesoproterozoic|Mesoproterozoic|||||||
24488|Sawpit Granodiorite|36937|6|Mentioned|p229|||||||||
24488|Sawpit Granodiorite|37570|4|Described|p121|||||||||
24488|Sawpit Granodiorite|37576|5|Briefly described|p8|||||||||
24488|Sawpit Granodiorite|39445|5|Briefly described|Table 2|||See also p72 & p148||||||16-FEB-19
24488|Sawpit Granodiorite|50200|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
24488|Sawpit Granodiorite|50211|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Grey, foliated, biotite granodiorite, tonalite and quartz diorite with abundant gneiss xenoliths.  Age: 1550-1560 Ma.||||||17-MAY-04
24488|Sawpit Granodiorite|68357|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Grey, foliated, biotite granodiorite, tonalite and quartz diorite with abundant gneiss xenoliths.|
24488|Sawpit Granodiorite|68410|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Shown as D2 1550 - 1560 Ma.|1560-1550 Ma||||Foliated, grey biotite granodiorite, tonalite and quartz diorite with abundant gneiss xenoliths.|
37864|Sawpit Supersuite|23291|4|Described|p88 Tb. 3.7|||Age: uncertain - Mesoproterozoic? (Rb-Sr age ca. 390Ma, Black & Holmes unpub. ms.). Intrudes Einasleigh Metamorphics; intruded by Blackman Gap and White Springs Supersuites. Geological Province: Georgetown Region.||||||08-JUL-15
26324|Saxby Granite|22460|6|Mentioned|Fig 1 p446.|||||||||
26324|Saxby Granite|22465|6|Mentioned|p934|||||||||
26324|Saxby Granite|22515|3|Fully described|Fig1p398,402|Calymmian||One pluton dated by U-Pb zircon as 1520 Ma.||||||
26324|Saxby Granite|22523|6|Mentioned|p364,Fig2p364,371|||||||||
26324|Saxby Granite|22667|6|Mentioned|Fig1 P234|||||||||
26324|Saxby Granite|22735|6|Mentioned|p282 Fig 1|Calymmian|Calymmian|spelled with a lower case (informal and misspelled) g in some places in text and on Fig 1.  Spelled correctly, with capital G elsewhere in text.||||||
26324|Saxby Granite|23519|5|Briefly described|p127|||See also page 112 Table 1.||||||
26324|Saxby Granite|23967|4|Described|p1334|Mesoproterozoic|Mesoproterozoic|Of Clonclurry Supersuite.  Intrudes Soldiers Cap Group.||||||
26324|Saxby Granite|24032|6|Mentioned|p12|||||||||
26324|Saxby Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
26324|Saxby Granite|24254|5|Briefly described|p17 Fig.1, p19 Fig.2|Proterozoic|Proterozoic|Geological Province: Eastern Fold Belt, Mount Isa Inlier.  Age: ca. 1530-1520 Ma.||||||
26324|Saxby Granite|24256|6|Mentioned|p48, p50 Fig.2|||Geological Province: Mount Isa Block.||||||
26324|Saxby Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
26324|Saxby Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
26324|Saxby Granite|37862|4|Described|p589|||||||||
26324|Saxby Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26324|Saxby Granite|38658|6|Mentioned|p153|||||||||
26324|Saxby Granite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26324|Saxby Granite|39445|6|Mentioned|Table 2|||||||||
26324|Saxby Granite|39496|4|Described|p15|||||||||
26324|Saxby Granite|40840|6|Mentioned|Map legend|||||||||
26324|Saxby Granite|41568|6|Mentioned|p19|||||||||
26324|Saxby Granite|43490|6|Mentioned|8|||U-Pb Zircon Age: 1520Ma||||||
26324|Saxby Granite|44195|6|Mentioned|p350|||||||||
26324|Saxby Granite|45161|5|Briefly described|p52|||||||||
26324|Saxby Granite|45166|5|Briefly described|p39|||||||||
26324|Saxby Granite|49009|2|Defined|p40|Proterozoic|Proterozoic|Originally mapped as part of the Williams Granite (Carter & Opik,1963).||||||15-MAR-07
26324|Saxby Granite|50100|5|Briefly described|p13 Fig.4, p21|Calymmian|Calymmian|Of the Williams Supersuite.||||||
26324|Saxby Granite|50536|5|Briefly described|p1.5, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite/Supersuite. Age: ~1520Ma (SHRIMP).||||||22-JUN-16
26324|Saxby Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
26324|Saxby Granite|61933|5|Briefly described|p169 Fig.1, p173|Mesoproterozoic|Mesoproterozoic|Age: 1530-1520 Ma.||||||
26324|Saxby Granite|61936|5|Briefly described|p200|||A-type, metaluminous, magnetite-bearing plutonic rocks of the Isan Orogeny. ||||||
26324|Saxby Granite|62047|6|Mentioned|p90, p91 Fig.2, p101,p102 |||Shown as Saxby granite, part of Williams Batholith p101. Paper discusses metamorphism associated with this unit.||||||
26324|Saxby Granite|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks.||||||
26324|Saxby Granite|64248|6|Mentioned|p33 Fig.1, p45|||||||||
26324|Saxby Granite|64249|5|Briefly described|p84 Fig. 2, p86, p90, p102, p104|Mesoproterozoic|Mesoproterozoic|Age: 1520 and 1536Ma, has a U-Pb zircon age of 1520+/-8Ma. Geological Province: Mount Isa Inlier.||||||
26324|Saxby Granite|64250|6|Mentioned|p10, p9 fig 1, p11 fig 3|||Cloncurry Fold Belt, Mount Isa Inlier.|1520 +/-8 Ma.|||||
26324|Saxby Granite|64251|6|Mentioned|p55, p56, p60|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
26324|Saxby Granite|65396|5|Briefly described|p4, p7, p11 Fig.6, p13, p21-22, p40, p53|Calymmian|Calymmian|See also p56, p61, p82, p84, p88, p97-99, p102-103, p106, p109, p114, p118, p120, p141-142, p156-157, p159-160, p162, p172-173, p175, p179, p213, p223-224, p241, p271-272, p274-276, p280-281, p283-285, p327, p344-345, p359-361, p364, p366, p438, p444-445, p455-491. Cloncurry Fold Belt: Williams-Naraku Batholith. Whole-rock geochemistry detailed. Intrusion age of 1527 +/- 3 Ma. Metamorphic effects detailed and illustrated. Magnetic susceptibility discussed. Occasionally referred to as Saxby Granites (eg p157). Appears as Saxby granite on p223 and p276. Magnetic and gravity worms discussed. Fluid inclusions studied. Stress partitioning and fluid flow models detailed.|1536 +/- 20 Ma, 1520 +/- 8 Ma (SHRIMP)||||Hornblende-biotite granite.|
26324|Saxby Granite|65755|5|Briefly described|p3, p13|||1530 - 1520 Ma||||||10-SEP-14
26324|Saxby Granite|66526|5|Briefly described|p36.|Proterozoic|Proterozoic|Mount Isa Province. It has associated small gabbro and dolerite bodies produced in the Saxby Event, ME 17 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1530 Ma.|||||
26324|Saxby Granite|66913|5|Briefly described|p171 fig 2|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2.||||||
26324|Saxby Granite|67323|4|Described|GIS attrib tbl, Solid Geology Map, p21|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. South of Cloncurry, Soldiers Cap Domain, Mount Isa Inlier. Williams Igneous Event. Also dated at 1536 +/- 12 Ma.|1520 +/- 8 Ma (Rubenach et al., 2008).|Williams Supersuite.||Intrudes the Soldiers Cap Group.|Porphyritic biotite, hornblende, and hornblende-biotite granite; minor pyroxene-bearing granite, non-porphyritic granite and aplite|
26324|Saxby Granite|67498|6|Mentioned|p918-920, p925 Fig.4, p927, 929-930, 932|||Intrudes Paleoproterozoic sedimentary successions.||Of the Williams-Naraku Suite.||||08-MAY-12
26324|Saxby Granite|69370|6|Mentioned|p306 Fig.1, p308 Fig.3|Calymmian|Calymmian|Intrudes Eastern Fold Belt.|1527 Ma.|||||
26324|Saxby Granite|69591|5|Briefly described|p51, p59|||Eastern Mount Isa Province; late Isan Orogeny.|1536 +/- 12 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.|||A-type granitoid.|
26324|Saxby Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|||Porphyritic biotite, hornblende, and hornblende-biotite granite; minor pyroxene-bearing granite, non-porphyritic granite and aplite.|05-MAY-16
26324|Saxby Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|||Porphyritic biotite, hornblende and hornblende-biotite granite; minor pyroxene bearing granite, non porphyritic granite and aplite.|
26324|Saxby Granite|71592|5|Briefly described|Appendix A.|||Soldiers Cap Domain, Mount Isa Orogen.|1536+/-12 Ma (U-Pb zircon SHRIMP)||||Granite.|
26324|Saxby Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
26324|Saxby Granite|73525|5|Briefly described|p4-5 Fig.2|Calymmian|Calymmian|Snake Creek-Soldiers Cape Domain.|1536+/-12 Ma crystallisation age||||Felsic intrusive.|
79951|Scalby Granite|71965|4|Described|p908-909,912-914|Fammenian|Fammenian|Geological province: Thomson Orogen. Of the Scalby Belt. S-type granite dated at 368.4+\-2.5 Ma (Kositcin et al., 2015). Effects of contact metamorphism with Glenroy Formation possibly represented by elevated magnetic response of the Glenroy Formation afjacent intrusion contact zones.|368.4+\-2.5 Ma|||Intrudes into Glenroy Formation.|Massive, coarse-grained, mottled pink/white/grey muscovite-biotite granite with altered cordierite.|
79951|Scalby Granite|71966|5|Briefly described|p991,998|Famennian|Famennian|Geological province:  Thomson Orogen. S-type granite (elevated ASI, K2O/Na2O, P2O5, low LREE, Th/U) probably associated with tectonics related with the New England Orogen to the east. Intersected in drillhole AOP Scalby 1, and samples analysed for SHRIMP U-Pb geochronology, and Lu and Hf isotopic analysis. Sample 2130082 yielded a 206Pb/238U age of 368.4+\-2.5 Ma, which is interpreted to record the igneous crystallisation age of this rock. Strong temporal relationship to granites on the Roma Shelf, which were interpreted to ahve crystallised between 360-355 Ma (Murray 1994). Hf and O isotopic anaylsis indicate uncommon patterns of of near-juvenile to juvenile EHF values, but supracrustal O isotope signatures, which may be explained by reworking of juvenile sediments sourced from nearby, Early Devonian juvenile magmatism, related to contraction during the Tabberabberan Orogeny.|368.4+\-2.5 Ma (crystallisation)|||||
36518|Scalded Flat complex|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 168.  I-Type.||||||
36516|Scalp Dam granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 165.||||||
36276|Scardons Volcanic Group|23291|3|Fully described|p38, p93 Tb. 3.9|Late Carboniferous|Late Carboniferous|Previously mapped as "Scardons Volcanics" and "Warby Volcanics". Geological Province: Georgetown Region.||||||08-JUL-15
36276|Scardons Volcanic Group|23430|6|Mentioned|p498|||||||||
36276|Scardons Volcanic Group|23497|6|Mentioned|p32||Permian|||||||
36276|Scardons Volcanic Group|23510|5|Briefly described|Map Legend||Early Permian|||||||
36276|Scardons Volcanic Group|23616|5|Briefly described|Table 3 p52|||Unconformably overlies McDevitt Metamorphics and Blackman Gap Complex (part of the Blackman Gap Supersuite); intruded by Late Carboniferous granitoids. Thickness: >400 m.||||||
36276|Scardons Volcanic Group|68405|5|Briefly described|Map Legend|Permian|Late Carboniferous|Kennedy Province. Early Permian ? minimum age. See map legend for constituent lithology.|||Includes Bulleringa Volcanic Subgroup, Warby Volcanic Subgroup.|Older than Brodies Camp Supersuite rocks. Younger than White Springs Supersuite rocks.||
36276|Scardons Volcanic Group|68553|6|Mentioned|Map legend|Permian|Carboniferous|Parts of this unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed and Newcastle Range Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk. Part also mapped under Pvk.||||||26-APR-13
36276|Scardons Volcanic Group|69593|5|Briefly described|p484-485, p510|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Possibly co-magmatic with Brodies Camp Supersuite. Sm-Nd isotope data tabulated.|290 Ma.||Bulleringa Volcanic Subgroup.||A-type.|
36276|Scardons Volcanic Group|70207|6|Mentioned|p82|||N of the Newcastle Range.|||||A-type.|
30710|Scheelite Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite (part of the Wonga Batholith). Intrudes the Argylla Formation. Age: 1760Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30710|Scheelite Granite|50536|5|Briefly described|p1.4, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.||||||07-NOV-08
30710|Scheelite Granite|73553|5|Briefly described|p73-74, p91, p97-100|||Mary Kathleen Domain. Wonga Igneous Subprovince, northern. Highly elongate intrusions extending ~15.6 km from north to south, maximum width of ~2 km, segmented by minor faults. Crops out as isolated bouldery knolls. Previously mapped as Wonga Granite subunit '1' in the south, subunit '2' in central bodies, and undivided Wonga Granite in the north (GSQ, 2018). General distribution adopted from Bastrakova et al (2001) with amended boundaries from detailed surface geology dataset (GSQ, 2018). Described previously by Bastrakova et al., (2001). Undated, apparent continuity with Mount Maggie Granite suggests age of ~1730 Ma. White to bluish tones in the south on radiometric images, becomes duller northwards. Subdued magnetic response.||||Intrudes Corella Formation, interpreted to intrude Argylla Formation, Magna Lynn Metabasalt|Foliated coarsely porphyritic biotite-amphibole monzogranite; fine-grained biotite monzogranite; pegmatite and intrusion breccia occur at contact with Corella Formation.|03-FEB-23
27231|Schreibers Granodiorite|22847|3|Fully described|p 43||Ordovician|Pb/U age 490 +/-6Ma||||||
27231|Schreibers Granodiorite|23422|5|Briefly described|p173, p210 Table 6.6|Ordovician|Late Cambrian|Of Schreibers Suite.||||||
27231|Schreibers Granodiorite|23430|4|Described|Table 14.2 p460.|Ordovician|Cambrian|490+/-6 Ma Zircon Pb/U. Also see p480. Ravenswood Batholith Province||||||
27231|Schreibers Granodiorite|42633|5|Briefly described|Table 1 P11|||Reserved as Schreibers Granite.||||||
27231|Schreibers Granodiorite|42750|2|Defined|p33|Early Ordovician|Late Cambrian|||||||
27231|Schreibers Granodiorite|43093|4|Described|Appendix 1|||Pb-U zircon age of 490+/-6Ma||||||
27231|Schreibers Granodiorite|43934|5|Briefly described|Map Legend||Ordovician|||||||
27231|Schreibers Granodiorite|62074|6|Mentioned|p2|Early Ordovician|Late Cambrian|N of Mount Leyshon.||||||
27231|Schreibers Granodiorite|62521|5|Briefly described|p6, p11, p26|Early Ordovician|Late Cambrian|Of Schreibers Suite. Age: ~490+/-6Ma. Geological Province: Ravenswood Batholith. Characterised by large compound quartz grains up to 10cm in diameter. See also p6, p11.||||||14-JAN-08
27231|Schreibers Granodiorite|68731|5|Briefly described|p146, p147, p151|Early Ordovician|Furongian|(Hutton and Crouch 1993a; Hutton et al. 1994a; Hutton and Rienks 1997). I-type granitoid in the Ravenswood Batholith.|490 +/- 6 Ma, U/Pb SHRIMP (Hutton et al. 1994a)||||Comprises medium- to high-K calc-alkaline granitoids.|
27231|Schreibers Granodiorite|71592|5|Briefly described|Appendix A.|||Macrossan Igneous Province, Thomson Orogen.|490+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
34667|Schreibers Suite|22847|6|Mentioned|p 10|||||||||
34667|Schreibers Suite|23422|4|Described|p173, p210 Table 6.6|Early Ordovician|Late Cambrian|U-Pb date, 490 +/- 6 Ma||||||06-DEC-11
34667|Schreibers Suite|23893|5|Briefly described|p13|Early Ordovician|Late Cambrian|||||||
34667|Schreibers Suite|62521|5|Briefly described|p1, p26|Middle Ordovician|Late Cambrian|Includes Schreibers Granodiorite. Geological Province: Ravenswood Batholith.||||||14-JAN-08
34667|Schreibers Suite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Brittany, Chipley, Columbia Creek (part), Hogsflesh and Lavery Creek Supersuites; the Sunburst Suite; the Lynwater Complex; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
37737|Schultz Sandstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Constance Sandstone.||||||
37737|Schultz Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Constance Sandstone. White to brown, friable, medium, coarse and very coarse grained to granule sandstone; platy, thinly laminated very fine grained sandstone and minor siltstone and shale.||||||
37737|Schultz Sandstone Member|65337|3|Fully described|p9 Fig.5, p38 Table 5.|Mesoproterozoic|Mesoproterozoic|New name. Northeast MOUNT DRUMMOND area. Includes siltstone lenses formerly (Sweet 1981) named Bowthorn Siltstone Member. Basal beds outcrop as spectacular, bare rocky platforms cut by deeply eroded joints; giant displaced blocks are common.||Unit in Constance Sandstone.||Disconformably overlies Wallis Siltstone Member. Is overlain by Mullera Formation.|Yellow to white, subfriable medium- to coarse-grained, well-sorted quartz sandstone; some granule layers; becomes medium-grained up-section. Very pure quartz sandstone with siliceous cement continues to top of Formation. Cross-bedded throughout.|
37737|Schultz Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Basal yellow to white, subfriable, medium- to coarse-grained well-sorted quartz sandstone; passes up into medium-grained, very pure quartz sandstone with siliceous cement.|
37737|Schultz Sandstone Member|67539|6|Mentioned|p14, p15 Fig.8|||Rawlings and others (2008). Equivalent to the new, reduced Constance Sandstone and therefore rendered obsolete.||||||
37737|Schultz Sandstone Member|68146|4|Described|p2, p6, p27-33, p35, p196-197, p211|||South Nicholson Region. A distinctive, tor-like outcropping unit. Described as "laterally equivalent" to Constance Sandstone, and is also presented on that page as Constance Sandstone-Schultz Sandstone[sic]; similar detrital zircon spectra. Whole-rock Sm-Nd isotopic data tabulated.|1577 +/- 21 Ma; maximum depositional age.|Basal Constance Sandstone.||Unconformably overlies Wild Cow Subgroup.|Fine- to medium-grained, well-sorted, quartz sandstone.|
37737|Schultz Sandstone Member|69434|4|Described|p19:2, 6|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. 120-over 600m thick. Shallow-marine deposits: upper shoreface to intertidal; may include braided fluvial.||Constance Sandstone.||Disconformably overlies Wallis Siltstone Member. Is overlain conformably by Mullera Formation.|White to brown, friable, medium, coarse and very coarse to granule sandstone; 220m-thick intercalated unit of platy, thinly laminated, very fine sandstone.|12-JUL-16
37737|Schultz Sandstone Member|69591|5|Briefly described|p52-53|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). High-energy fluvial deposits.||Constance Sandstone.||Unconformably overlies Wallis Formation. Is overlain unconformably by Elizabeth Sandstone.|Resistant sandstone with a basal layer of coarse cobble-to-boulder conglomerate.|
37737|Schultz Sandstone Member|71369|3|Fully described|p5-7, p12, p19-20, p23-31, p33, p36, p50|Mesoproterozoic|Mesoproterozoic|See also p1. Rawlings et al. (2008). Their description, having abandoned the Bowthorn Siltstone Member, coincided with the entire span of the Constance Sandstone of Carter et al. (1961). Redefinition in this study has this Member applied only to the lower part of the Constance Sandstone. South Nicholson Basin. Up to 700-1000m thick; c.200m in the type section, whose base is 14km SE of Bowthorn homestead. Proximal fluvial deposits. Forms distinctive slabby outcrops. Facies discussed in detail.||Constance Sandstone.||Unconformably overlies Wallis Formation (Wild Cow Subgroup) and Termite Range Formation (McNamara Group). Is overlain by Bowthorn Member (and locally by Elizabeth Sandstone unconformably).|Thick-bedded, pink-brown to red, mainly granule-rich but also pebbly to cobbly sandstone lacking fine-grained interbeds. Basal conglomerate lenses, and distinctive sandstone with no partings or interbeds thus forming very large blocks in outcrop.|20-FEB-18
37737|Schultz Sandstone Member|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1577+/-21 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
37737|Schultz Sandstone Member|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72526|5|Briefly described|p33-34.|Mesoproterozoic|Mesoproterozoic|Of Rawlings et al., 2008 and Sweet, 2017. Along with Bowthorn Member this unit is interpreted as part of the Constance Sandstone in Queensland. [Current status of this unit is unclear. Not shown in p8 figure.]||Of Constance Sandstone of Rawlings et al., 2008 and Sweet, 2017.||Probably underlies Bowthorn Member.||
37737|Schultz Sandstone Member|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|||Constance Sandstone||Overlies Wallis Sandstone Member and underlies Mullera Formation.||
37737|Schultz Sandstone Member|72919|6|Mentioned|p5, p47-48, p94-95|Ectasian|Calymmian|Included in Constance Sandstone in both NT and QLD, but the Accident Subgroup in NT (Rawlings et al., 2008) and the Wild Cow Subgroup in QLD (Sweet, 2017). Previous maximum depositional age in QLD of 1577 +/- 21 Ma from Carson et al. (2011).|1577 +/- 21 Ma (QLD)|Constance Sandstone||Overlain by Mullera Formation. Underlain by Wallis Sandstone Member.||
37737|Schultz Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard. Known oil show.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Unconformably underlain by Wallis Formation (Wild Cow Subgroup).||
22822|Scoop Holes Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22822|Scoop Holes Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 198.  I-Type.||||||
22822|Scoop Holes Granodiorite|43093|6|Mentioned|Fig.47,Table 10.|||see also Scoop Hills Granodiorite in Appendix 1.||||||
22822|Scoop Holes Granodiorite|43259|4|Described|Appendix 1,p29.|Early Devonian|Late Silurian|||||||
22822|Scoop Holes Granodiorite|43936|5|Briefly described|Map legend|Devonian|Silurian|||||||
83678|Scorpio Seam|73305|6|Mentioned|p551, p552 Fig.4, p554 Tb.2|Late Permian|Late Permian|Bowen Basin. Second-order coal seam within the Fair Hill Formation split from the FH1 seam [Fair Hill Seam]. 2.6 to 5.0 m thick. Abbreviated as Scorpio.||Fair Hill Formation|||Coal seam.|
33204|Scotia Coal Member|64856|5|Briefly described|p42, p58-61|Late Permian|Late Permian|Bowen Basin. Basal Member of Burunga Formation. Gradational contact with underlying Banana Formation. Contains sandstone, shale, siltstone, coal seams, tuff. Age implied from Burunga Fm.| | ||||29-NOV-17
33204|Scotia Coal Member|64857|5|Briefly described|p119-121, p113 Fig.3|Late Permian|Late Permian|Northeastern Bowen Basin. Overlies Banana Formation. Of Burunga Formation?||||||
33204|Scotia Coal Member|64858|5|Briefly described|p182, p180 Fig.2|Late Permian|Late Permian|Referred to also as Scotia Member (p181, 192). Member of the Burunga Formation.||||||30-NOV-09
33204|Scotia Coal Member|64859|5|Briefly described|p196, 225|Permian|Permian|Of Burunga Formation. Oil and gas source rocks.||||||13-NOV-15
33204|Scotia Coal Member|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Basal unit in the Burunga Formation, Taroom Trough, Bowen Basin. Overlies Banana Formation.||||||22-MAR-12
33204|Scotia Coal Member|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Taroom Trough. Underlies Burunga Formation, overlies Banana Formation.||||||
33204|Scotia Coal Member|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
33204|Scotia Coal Member|65115|5|Briefly described|p415, 416, 418, Fig 2 p403|Tatarian|Tatarian|of the Burunga Formation. Shown as Scotia Member in Fig. 2. Deltaic. Overlies the Banana Formation in the Taroom Trough, Bowen Basin. Part of Supersequence E.||||||
33204|Scotia Coal Member|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Burunga Formation and overlies the Banana Formation in the Taroom Trough, Bowen Basin.||||||
33204|Scotia Coal Member|65119|6|Mentioned|Fig 6 p512|||Present in the Wandoan 1 well.||||||07-MAR-12
33204|Scotia Coal Member|66615|6|Mentioned|p2 Fig.1, p6|||Southern Taroom Trough, Bowen Basin.||Of the Burunga Formation.||||
33204|Scotia Coal Member|68679|5|Briefly described|p382|Permian|Permian|Beeston and Green (1995). E Taroom Trough, Bowen Basin. Prograding delta complex deposits.||Burunga Formation.|||Sandstone, mudstone, siltstone, coal and tuff.|
33204|Scotia Coal Member|72297|5|Briefly described|p744|||Bowen Basin. Sandstones in this unit are hydrocarbon reservoirs.||Burunga Formation.||||
41927|Screaming Creek Gabbro|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Medium- to very coarse-grained, commonly layered, poikolitic hornblende gabbro and leucogabbro; intruded by andesite, basalt and minor microgranite dykes. Part of the Urannah Batholith.||||||
41927|Screaming Creek Gabbro|65388|2|Defined|p381-382, 135, 362, 364, 365, 372, 380|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Probably intrudes the Pisgah Igneous Complex. Mainly dark green to black, very coarse-grained, equigranular olivine-clinopyroxene-hornblende gabbro.||||||
23959|Scrubby Creek Rhyolite|23291|4|Described|p42, p91 Tb. 3.9|Late Carboniferous|Late Carboniferous|Thickness: 700m. Included in the Cumberland Range Volcanic Group for ease of description. Geological Province: Georgetown Region.||||||19-MAY-15
23959|Scrubby Creek Rhyolite|23430|6|Mentioned|p499|||||||||
23959|Scrubby Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V12. Assumed to be I-Type.||||||
23959|Scrubby Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23959|Scrubby Creek Rhyolite|40542|6|Mentioned|p97|||||||||
23959|Scrubby Creek Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Cumberland Range Volcanic Group.||||||
23959|Scrubby Creek Rhyolite|43740|4|Described|p21|||||||||
23959|Scrubby Creek Rhyolite|50595|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of the Cumberland Range Volcanic Group. Underlies: Namul Dacite.||||||01-JUL-04
23959|Scrubby Creek Rhyolite|68352|5|Briefly described|Map legend.|Late Carboniferous|Early Carboniferous|Kennedy Province. Cumberland Cauldron. Eleven facies associations are mapped separately.||Unit in Cumberland Range Volcanic Group.||Is overlain conformably by Namul Dacite.|Rhyolitic ignimbrite; basaltic andesite; tuffaceous sandstone and siltstone, sandstone breccia, algal limestone and granite-boulder conglomerate; sublithic sandstone, flaggy siltstone and mudstone; feldspathic and volcanilithic sandstones.|
38224|Scrubby Creek Suite|23422|4|Described|p211 Table 6.7|||||||||
38224|Scrubby Creek Suite|68731|5|Briefly described|p147|Late Ordovician|Middle Ordovician||455 +/- 10 Ma||||Hornblende-bearing granitoid.|
81020|Scrubby Top Granite|68679|6|Mentioned|p367 Fig.5.58, p368|||Geochemical plots. Grouped with Early Permian Thunderbolt Granite. [Possibly of Thunderbolt Suite].||||||30-APR-19
81020|Scrubby Top Granite|69594|6|Mentioned|p570-571 Figs.7.44-45|||Northern Urannah Batholith. Geochemistry plots.||||||
81020|Scrubby Top Granite|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Buff to pale brown, fine-grained, even-grained, leucocratic biotite monzogranite; miarolitic; partly granophyric; with traces of titanite and allanite.|
22826|Scrufflem Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Djungan Volcanic Subgroup of Featherbed Volcanic Group.||||||
22826|Scrufflem Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).  Rhyolitic ignimbrite.||||||15-JUN-06
22826|Scrufflem Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Djungan Subgroup.||||||
22826|Scrufflem Rhyolite|43259|6|Mentioned|Appendix 1,p11.||Early Permian|||||||
22826|Scrufflem Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
22826|Scrufflem Rhyolite|43626|2|Defined|p59||Early Permian|Age: between 281+/-2 Ma and 289+/-10 Ma||||||
22826|Scrufflem Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Djungan Volcanic Group (Featherbed Volcanic Group). Geological Province: Kennedy Province. Dark grey to greenish grey, moderately to very crystal-rich, rhyloitic-ignimbrite, with variably reacted granite; poorly developed pumice foliation in places.||||||
22826|Scrufflem Rhyolite|60425|5|Briefly described|p46 Tb. 3|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
23960|Scurvy Creek Meta-arenite|22557|6|Mentioned|p567,569|||||||||
23960|Scurvy Creek Meta-arenite|22982|5|Briefly described|p269 Fig.4|||||||||
23960|Scurvy Creek Meta-arenite|23078|5|Briefly described|p708|||||||||
23960|Scurvy Creek Meta-arenite|42747|5|Briefly described|p33, Fig.3|||of Anakie Metamorphic Group||||||
23960|Scurvy Creek Meta-arenite|43204|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|Neoproterozoic or Early Cambrian. Anakie Inlier.||||||23-DEC-11
23960|Scurvy Creek Meta-arenite|43213|3|Fully described|p8, p20-23, p25, p43-45, p130-140, p203|||See also p236, p240, p245. Named after Scurvy Creek. Outcrop and type areas, and geophysical properties, are described. Structurally underlies Bathampton Metamorphics, but could be a lower-grade equivalent of Wynyard Metamorphics: if so, the contact must be tectonic, possibly a thrust. Deformation structures and chemical analyses detailed. Is unconformably overlain by Permian rocks of the Moorlands and Blair Athol Basins.||Unit in Anakie Metamorphic Group.||Structurally overlies Hurleys Metamorphics.|Generally well-foliated, green, chloritic, labile meta-arenite interlayered with subordinate phyllite or fine-grained mica schist.|
23960|Scurvy Creek Meta-arenite|43861|2|Defined|25, 30, 31|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group. Overlies Hurleys Metamorphics, underlies Bathampton Metamorphics||||||
23960|Scurvy Creek Meta-arenite|66085|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Unit in Anakie Metamorphic Group. Green, fine- to medium-grained, foliated, labile meta-arenite (chlorite-muscovite-feldspar-quartz schist) and generally subordinate phyllite and fine-grained mica schist.||||||
23960|Scurvy Creek Meta-arenite|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.||Conformably overlies Hurleys Metamorphics.|Green, fine- to medium-grained, foliated, labile meta-arenite (chlorite-muscovite-feldspar-quartz schist) and generally subordinate phyllite and fine-grained mica schist.|
23960|Scurvy Creek Meta-arenite|68731|5|Briefly described|p120 Fig 3.6, p122, p126, p133|Cambrian Series 3||K-Ar ages for minimum age of deformatin/metamorphism between 495-502 from phyllite (Withnall et al. 1996).|~ 500 Ma, K-Ar|Of the Anakie Metamorphic Group.||Underlain by the Hurleys Metamorphics. Structurally overlain by the Bathampton Metamorphics, but Scurvy may be younger.|Comprises labile meta-arenite and less abundant phyllite or fine-grained mica schist.|20-JUL-20
23960|Scurvy Creek Meta-arenite|68900|5|Briefly described|p6, p10|||Drummond Basin. Potential correlative of the Wynyard Metamorphics.||||Faulted against the Bathampton Metamorphics.|Well-foliated, green, chloritic, labile meta-arenite interlayered with phyllite.|
23960|Scurvy Creek Meta-arenite|70740|5|Briefly described|p13|||||||Eqvuialent to the Anakie Metamorphic Group.||
23960|Scurvy Creek Meta-arenite|70749|5|Briefly described|p43|Cambrian|Neoproterozoic|Anakie Province.||Anakie Metamorphic Group.||||
23960|Scurvy Creek Meta-arenite|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Anakie Province, Thomson Orogen.||||||
34136|Sedgeford Formation|22604|2|Defined|p438, Fig.3 p440|Middle Devonian|Emsian|See also p440, p442, Fig.1 p438||||||
34136|Sedgeford Formation|22800|6|Mentioned|Fig.7 p586|Middle Devonian|Middle Devonian|||||||
34136|Sedgeford Formation|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|||||||
34136|Sedgeford Formation|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Ukalunda. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
34136|Sedgeford Formation|67402|6|Mentioned|p239|Middle Devonian|Early Devonian||||||Siliciclastic sediments.|
34136|Sedgeford Formation|68411|5|Briefly described|Map Legend|Devonian|Devonian|Drummond Basin||||Unconformably overlain by the Silver Hills Volcanics|Medium-grained, well sorted quartzose sandstone and pebbly sandstone; minor fine to medium-grained, calcareous sandstone and rare limestone.|
34136|Sedgeford Formation|68553|6|Mentioned|Map legend|Devonian|Devonian|This unit, as well as the Ukalunda Formation, the Douglas Creek Limestone, the Theresa Creek and Dunstable Volcanics, and unnamed Devonian sedimentary and volcanic units, are all mapped under the symbol, Da.||||||
34136|Sedgeford Formation|68731|5|Briefly described|p171, p174, p177 Fig 3.91|Middle Devonian|Middle Devonian|Henderson, Davis and Cook (1995). > 1 km thick succession. Transgressive deposit.|||||Comprises two informal members - a lower non-marine sandstone with Lepidodendron stem and leaf remains, and fish debris; conformably overlain by a richly fossiliferous marine sandstone with limestone beds.|18-JUL-14
34136|Sedgeford Formation|68900|4|Described|p4, p34-p35|Devonian|Devonian|Drummond Basin. Exposed on the western side of the Mount Beaufort Anticline. First described by Henderson et al (1995) who subdivided it into two informal units. This unit is recessive though some sandstones outcrop well. Lithology and biostratigraphy are discussed in detail. Deposited in a shallow marine or fluvial environment.||||Faulted against the Silver Hills Volcanics and Anakie Metamorphic Group.|Medium-grained, well-sorted quartzose sandstone and pebbly sandstone. Rare thin, pebble conglomerate beds. Fine to medium-grained, well-sorted calcareous sandstone.|
34136|Sedgeford Formation|69379|5|Briefly described|map legend|Devonian|Devonian|Drummond Basin|||||Medium-grained, well-sorted quartzose sandstone and pebbly sandstone; minor fine to medium-grained, calcareous sandstone and rare limestone|08-SEP-14
34136|Sedgeford Formation|69592|6|Mentioned|p229|Devonian|Devonian|Scattered remnants in central QLD, developd on Thomson Orogen basement.||||||
25469|Sefton Metamorphics|22533|6|Mentioned|p47,p56||Neoproterozoic|||||||
25469|Sefton Metamorphics|22543|6|Mentioned|p62|Cambrian|Neoproterozoic|Assigned to Iron Range Province||||||
25469|Sefton Metamorphics|22811|5|Briefly described|p597, Fig.2 p598|Mesoproterozoic|Mesoproterozoic|Of Iron Range Province. Max age: Late Mesoproterozoic.||||||
25469|Sefton Metamorphics|23420|5|Briefly described|p 142 table 4.4||Stenian|Also see p124. Age: younger than 1133Ma (detrital zircon) In the Iron Range Province. Mount Carter, Bolt Head and Iron Range Schists were renamed Sefton Metamorphics.||||||
25469|Sefton Metamorphics|23425|5|Briefly described|Fig 9.4 p367|||||||||
25469|Sefton Metamorphics|23429|5|Briefly described|p435|||||||||
25469|Sefton Metamorphics|23430|4|Described|p458-459||Proterozoic|The only mapped unit of the Iron Range Province.||||||
25469|Sefton Metamorphics|23431|5|Briefly described|p535|||Iron Range Province.||||||
25469|Sefton Metamorphics|29960|6|Mentioned|p2|||||||||
25469|Sefton Metamorphics|30257|5|Briefly described|p286|||See also date on p301.||||||
25469|Sefton Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25469|Sefton Metamorphics|32528|5|Briefly described|Table 2|||||||||
25469|Sefton Metamorphics|32563|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25469|Sefton Metamorphics|33226|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
25469|Sefton Metamorphics|33773|6|Mentioned|p10|||||||||
25469|Sefton Metamorphics|33880|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25469|Sefton Metamorphics|33882|4|Described|Table 1|||Described p8||||||
25469|Sefton Metamorphics|34581|2|Defined|p130|Precambrian|Precambrian|See also pp132,134,135,140||||||
25469|Sefton Metamorphics|37570|4|Described|p122|||||||||
25469|Sefton Metamorphics|39445|5|Briefly described|p44|||See also Table 2||||||
25469|Sefton Metamorphics|42327|5|Briefly described|p14|||||||||
25469|Sefton Metamorphics|42360|5|Briefly described|p246|||||||||
25469|Sefton Metamorphics|42550|4|Described|p6|||||||||
25469|Sefton Metamorphics|42640|5|Briefly described|p9|||||||||
25469|Sefton Metamorphics|42650|6|Mentioned|p13|||||||||
25469|Sefton Metamorphics|43124|5|Briefly described|p28|||||||||
25469|Sefton Metamorphics|43708|6|Mentioned|Fig.1b,p3||Proterozoic|||||||
25469|Sefton Metamorphics|43775|6|Mentioned|p27||Proterozoic|||||||
25469|Sefton Metamorphics|43811|6|Mentioned|p191|||||||||
25469|Sefton Metamorphics|45076|3|Fully described|p87|||||||||
25469|Sefton Metamorphics|49769|6|Mentioned|Fig.1,p2|||||||||
25469|Sefton Metamorphics|63866|5|Briefly described|p81|||Rocks of this group outcrop around Mount Carter, between Pascoe River and the Iron Range, along headlands of Temple Bay and in the Bowden area. Numeric age derived from Blewett et al., 1998.|c. 1200 Ma (maximum depositional age)||||Fine-grained schist and quartzite, slate/phyllite, greenstone, limestone, marble and calc-silicate rock.|
25469|Sefton Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Iron Range Province.||||||
25469|Sefton Metamorphics|69591|5|Briefly described|p74 Fig.2.71, p80, p111|Neoproterozoic|Neoproterozoic|The only mapped unit in Iron Range Province, Coen Inlier, Etheridge Province. Crops out in the Mount Carter and Iron Range areas (other locations listed). Total thickness unknown, but <2000m. Underwent four phases of deformation (briefly described). The age is given as Neoproterozoic (?); a sponge spicule and other organic matter suggests some of the unit is Paleozoic.|~1130 Ma (MDA: Blewett et al., 1998).||||Ironstone (quartz-haematite schist and magnetite quartzite), schistose conglomerate, graphitic phyllite, quartzite, calc-silicate, marble and greenstone. Sub-greenschist to greenschist grade metamorphism.|
25469|Sefton Metamorphics|70207|4|Described|p2-3, p11, p125-148|Cambrian|Neoproterozoic|The only constituent of the Iron Range Province, Coen Inlier, Eastern Cape York. At least four deformations. Contains a (Paleozoic) sponge spicule in recrystallised limestone. Intruded by granitoids c.408 Ma. Three samples yield significantly different maximum depositional ages and provenance spectra (Kositcin et al., 2015), indicating need for more geological mapping and geochronology in that area.|1648.6 +/- 4.5 Ma; 992 +/- 29 Ma; 401 +/- 15 Ma.|||Is intruded by Weymouth and Kintore Granites and Blue Mountains Adamellite.|Mainly quartz-muscovite schist, with hematite schist, magnetite schist, phyllite, calc-silicate rocks, marble and greenstone; metamorphosed to mainly sub-greenschist and greenschist facies (locally amphibolite).|
25469|Sefton Metamorphics|70673|4|Described|p1, p3, p10, p71-76|||Willmott et al. (1973). Iron Range Province, eastern Cape York Peninsula. Said to have an informal name of Peninsula Hope Schist. Maximum depositional age; significantly younger than previous MDA determinations (described). Intruded by Silurian-Devonian granites of the Pama Igneous Association.|785 +/- 29 Ma.||||Quartzite, magnetite quartzite, quartz-hematite schist, metagreywacke, argillite, phyllite, slate, phyllitic schist, quartz-muscovite schist, greenstone, recrystallised schistose limestone and other calc-silicate rocks.|
25469|Sefton Metamorphics|71031|5|Briefly described|p5-p7, p13, p89-p90, p92-p95|||Iron Range Province. A maximum depositional age for the protolith of a sample was interpreted at 969 +/- 15 Ma.|||||Mainly quartz-muscovite schist. Includes biotite-garnet schist.|
25469|Sefton Metamorphics|71592|5|Briefly described|Appendix A.|||Iron Range Province. Eleven age determinations are given, for MDA, provenance clusters, Pb loss, metamorphism and "significance unknown".|785+/-29 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite, conglomerate, mica schist, schist.|
25469|Sefton Metamorphics|71792|1|Redefined|p3, p5-p6, p8, p13-p16|Cambrian|Neoproterozoic|Iron Range Province. This unit is named for the Sefton Creek in the Coen 1:250k sheet. The type area is defined as 5km to the east and west of a central location in the Iron Range (12.7167'S, 143.28'3333E (Whitaker and Willmott, 1968). Originally defined by Trail et al (1969) who identified three units: Mount Carter Schist, Iron Range Schist and Bolt Head Schist based on earlier worker by BHP geologists (Reid, 1959). Willmott et al. 1973 abandoned this subdivision and combined the units into one formation together with a lens of greenstone. The unit is redefined here to include two informal subunits which are described. Cambrian upper age is uncertain. The formation is difficult to access and rocks are generally deeply weather and very poorly exposed. This formation forms a belt of north-striking, hilly country to the east of the McIlwraith Range. This belt is ~40km long and up to 12km wide. Total thickness of 2000m was reported by Teluk (1984). Maximum depositional ages range from 785, 969, 992 to 1201 Ma and are SHRIMP U-Pb ages from Kositcin et al., 2015 and Blewett et al., 1998. MDA of 1648+/-4.5 Ma (Kositcin et al., 2015) now included in Coen Metamorphic Group on the basis of age. See also p18-p19, p31-p32, p59.|||||Muscovite-quartz schist, quartzite, phyllite, feldspathic schist, magnetite quartzite, greenstone, amphibolite, calc-silicate rocks and hematite schist.|
25469|Sefton Metamorphics|71849|6|Mentioned|p183|||Contains significant Au occurrences at Iron Range, near Portland Roads.||||||
25469|Sefton Metamorphics|71853|5|Briefly described|Map legend.|Cambrian|Neoproterozoic|The three facies are mapped separately.|||||Muscovite-quartz schist, quartzite, phyllite, feldspathic schist, magnetite quartzite, greenstone, amphibolite, schistose, limestone, calc-silicate rocks. Greenstone. Hematite schist horizon.|
25469|Sefton Metamorphics|72983|6|Mentioned|p5-6, p91, p93, p97, p100, p110|||New ages led to two mapped outcrops of this unit being reassigned to the Yarraden Schist. Detrital zircon geochronology typically have a significant Grenvillian (1300-900 Ma) to Neoproterozoic component.||||||
25469|Sefton Metamorphics|73083|6|Mentioned|p56-57|Neoproterozoic|Neoproterozoic|||||||
25469|Sefton Metamorphics|73387|6|Mentioned|p1, p33, p36|Neoproterozoic|Mesoproterozoic|Iron Range Province. Maximum depositional age of 1648.5 +/- 4.5 Ma was reported by Kositcin et al. (2015) but a much younger MDA of 785 +/- 29 Ma was reported by Cross et al. (2016).|785 +/- 29 Ma, 1648.5 +/- 4.5 Ma|||||
80778|Selina Creek Granodiorite|73029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Pale grey, fine to medium-grained, uneven-grained to slightly porphyritic hornblende-biotite granodiorite; with minor titanite.|
25471|Selwyn Supergroup|23333|5|Briefly described|1114 Fig.1|||||||||
25471|Selwyn Supergroup|41791|6|Mentioned|p266|||||||||
25471|Selwyn Supergroup|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||
25471|Selwyn Supergroup|61926|6|Mentioned|p71 Fig. 1|||Mentioned only in the context of undivided rocks. Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
25471|Selwyn Supergroup|61936|5|Briefly described|p190 Fig. 3|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. ||||||
22830|Sentinel Range Igneous Complex|23076|5|Briefly described|p727|||||||||
22830|Sentinel Range Igneous Complex|23291|6|Mentioned|p45|||Geological Province: Georgetown Region.||||||08-JUL-15
22830|Sentinel Range Igneous Complex|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Age: 303 +/- 2Ma, K-Ar. Part Ootann Supersuite, part biotite-hornblende granodiorite, quartz diorite (Almaden Supersuite?)part Almaden Supersuite?||||||
22830|Sentinel Range Igneous Complex|24485|5|Briefly described|p52 Tb.8|Late Carboniferous|Late Carboniferous|Age: 303 +/- 2Ma (K-Ar, biotite). Parent: Ootann Supersuite||||||
22830|Sentinel Range Igneous Complex|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
22830|Sentinel Range Igneous Complex|43083|5|Briefly described|p256|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
22830|Sentinel Range Igneous Complex|43087|2|Defined|p24|Late Carboniferous||K-Ar age of 303+/-2 Ma||||||
22830|Sentinel Range Igneous Complex|43259|4|Described|Appendix 1,p37.||Carboniferous|K-Ar biotite age is 302+/-2 Ma.||||||
22830|Sentinel Range Igneous Complex|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Felsic part of the Ootann Suite (Ootann Supersuite). Age: 303+/-2Ma (K-Ar). I-type. Mainly white to pale grey, fine-grained, porphyritic (hornblende-) biotite granite; accessory minerals; minor aplite -- detailed lithological description included.||||||07-FEB-11
22830|Sentinel Range Igneous Complex|69593|6|Mentioned|p486|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Has evidence of magma mixing.||||||
36634|Settlement Pocket granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 498.  I-Type.||||||
75608|Seventy Creek Granite|69594|5|Briefly described|p567 Fig.7.39|Cretaceous|Cretaceous|Bowen-Mackay region. Geochemical plot.||||||
23961|Seventy Mile Range Group|22543|6|Mentioned|p62|Early Ordovician|Late Cambrian|assigned to the Thalanga Province||||||
23961|Seventy Mile Range Group|22611|5|Briefly described|P186|Late Cambrian|Early Ordovician|||||||
23961|Seventy Mile Range Group|22621|6|Mentioned|p203,4,6,17|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|22630|6|Mentioned|p7 Fig.3|Early Ordovician|Late Cambrian|Thalanga Province||||||
23961|Seventy Mile Range Group|22675|4|Described|p13|||||||||
23961|Seventy Mile Range Group|22844|6|Mentioned|Fig3  p8,39,40,51|||||||||
23961|Seventy Mile Range Group|22847|4|Described|p 7|Early Ordovician|Late Cambrian|||||||
23961|Seventy Mile Range Group|23032|6|Mentioned|p14|||||||||
23961|Seventy Mile Range Group|23049|6|Mentioned|p9|||||||||
23961|Seventy Mile Range Group|23082|5|Briefly described|p686|Early Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|23083|5|Briefly described|p681|||||||||
23961|Seventy Mile Range Group|23278|5|Briefly described|p80, Fig1p81|Ordovician|Cambrian|(Henderson, 1986).||||||
23961|Seventy Mile Range Group|23291|6|Mentioned|p34|||Geological Province: Charters Towers Region.||||||
23961|Seventy Mile Range Group|23318|4|Described|p392 Fig.1|Ordovician|Cambrian|In the Mount Windsor Subprovince.||||||07-FEB-07
23961|Seventy Mile Range Group|23422|4|Described|p170, p206 Table 6.3|Ordovician|Late Cambrian|Geological Province: Thalanga Province.||||||
23961|Seventy Mile Range Group|23424|5|Briefly described|p345|||Charters Towers Region. May correlate with Balcooma Metavolcanics and Lucky Creek Group.||||||
23961|Seventy Mile Range Group|23430|4|Described|p462 p469-470|||Formed in back-arc extensional setting. Thalanga Province.||||||
23961|Seventy Mile Range Group|23431|5|Briefly described|p537|||||||||
23961|Seventy Mile Range Group|23432|5|Briefly described|p548|||||||||
23961|Seventy Mile Range Group|23504|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|23505|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|23764|5|Briefly described|p340|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|23852|5|Briefly described|p816|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|23893|6|Mentioned|p12|||||||||
23961|Seventy Mile Range Group|23940|5|Briefly described|p917 Fig. 3|Early Ordovician|Late Cambrian|||||||
23961|Seventy Mile Range Group|23950|5|Briefly described|p1134 Fig.1|Cambrian|Cambrian|||||||
23961|Seventy Mile Range Group|23952|5|Briefly described|p1176 Fig.1|Early Ordovician|Late Cambrian|Geological Province: Mount Windsor subprovince||||||
23961|Seventy Mile Range Group|23988|5|Briefly described|p19 Fig.10|Early Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|24035|5|Briefly described|p3 Fig. 1|Ordovician|Cambrian|Includes Rollston Range, Trooper Creek, Pubbler Creek Formations and Mount Windsor Volcanics.||||||
23961|Seventy Mile Range Group|24334|6|Mentioned|p47|||||||||
23961|Seventy Mile Range Group|37765|4|Described|p7|||||||||
23961|Seventy Mile Range Group|38658|6|Mentioned|p152|||||||||
23961|Seventy Mile Range Group|39445|5|Briefly described|p66|||Correlation with Cape River Beds||||||
23961|Seventy Mile Range Group|40746|3|Fully described|p344|||||||||
23961|Seventy Mile Range Group|40787|6|Mentioned|p321|||||||||
23961|Seventy Mile Range Group|40915|6|Mentioned|p113|||||||||
23961|Seventy Mile Range Group|40961|6|Mentioned|p241|||||||||
23961|Seventy Mile Range Group|41668|5|Briefly described|p6|||||||||
23961|Seventy Mile Range Group|41675|6|Mentioned|p52|||||||||
23961|Seventy Mile Range Group|41774|6|Mentioned|p29|||||||||
23961|Seventy Mile Range Group|41805|6|Mentioned|p26|||||||||
23961|Seventy Mile Range Group|41806|6|Mentioned|p45|||||||||
23961|Seventy Mile Range Group|42279|6|Mentioned|p17|||||||||
23961|Seventy Mile Range Group|42407|5|Briefly described|p34|||||||||
23961|Seventy Mile Range Group|42474|6|Mentioned|p28|||||||||
23961|Seventy Mile Range Group|42633|6|Mentioned|p14|||||||||
23961|Seventy Mile Range Group|42747|6|Mentioned|p34|||||||||
23961|Seventy Mile Range Group|42750|6|Mentioned|p35, p43, p44|||||||||
23961|Seventy Mile Range Group|43093|4|Described|p12|Early Ordovician|Late Cambrian|||||||
23961|Seventy Mile Range Group|43103|5|Briefly described|p17, Fig.6.|||||||||
23961|Seventy Mile Range Group|43213|5|Briefly described|p61-62, p65|Early Ordovician|Late Cambrian|Henderson (1986). Lolworth-Ravenswood Province. Not a correlative of Anakie Metamorphic Group, as that unit was metamorphosed in the Cambrian. Represents a volcanic arc related to convergence and subduction.|||||A sequence of calc-alkaline volcanic and clastic sedimentary rocks that host important VHMS mineralisation.|
23961|Seventy Mile Range Group|43259|6|Mentioned|Appendix 1,p7.|Ordovician|Cambrian|Upper Cambrian - Lower Ordovician in age.||||||03-DEC-13
23961|Seventy Mile Range Group|43391|5|Briefly described|Map legend|Ordovician|Cambrian|Geological Province: Lolworth-Ravenswood Block.  Includes the Mount Windsor Volcanics.||||||23-JUN-04
23961|Seventy Mile Range Group|43706|5|Briefly described|p14|||||||||
23961|Seventy Mile Range Group|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|43936|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|50153|5|Briefly described|p2, p4|Early Paleozoic|Early Paleozoic|Of Ravenswood Arch (Lolworth Ravenswood Block). Metamorphic sediments and volcanics, intruded by Early to Mid Ordovician granitoid plutons|||Includes the Mount Windsor Volcanics|||
23961|Seventy Mile Range Group|50552|5|Briefly described|p1044|Ordovician|Cambrian|In Lolworth-Ravenswood Terrane.||||||
23961|Seventy Mile Range Group|60659|5|Briefly described|p9, p12|Early Ordovician|Late Cambrian|Includes Rollston Range Formation. Comprises sublabile to labile clastic sedimentary rocks and felsic to intermediate lavas and fragmental volcanic rocks. See also p50 Fig. 2.||||||07-FEB-11
23961|Seventy Mile Range Group|61211|5|Briefly described|p262, p272 Fig. 16|Early Ordovician|Cambrian|Contains Lancefieldian to Chewtonian fossils. Age: ca.488-472Ma.||||||
23961|Seventy Mile Range Group|62074|5|Briefly described|p1-3|Early Ordovician|Late Cambrian|Part of the basement to Drummond Basin. Assigned to the Thalanga Province; form a roughly E-W belt across S margin of Lolworth-Ravenswood Block.|||||Sedimentary rocks and felsic to intemediate volcanic rocks.|
23961|Seventy Mile Range Group|62075|5|Briefly described|p7-9|Ordovician|Cambrian|Part of the basement in the Lolworth-Ravenswood terrane.|||||Subgreenschist to greenschist facies volcanic and sedimentary rocks.|
23961|Seventy Mile Range Group|62470|5|Briefly described|p181 Fig. 1|Ordovician|Cambrian|Includes: Puddler Creek, Mount Windsor, Trooper Creek and Rollston Creek Formations.||||||07-FEB-11
23961|Seventy Mile Range Group|62521|5|Briefly described|p2, p12|Early Ordovician|Late Cambrian|Intruded by units of the Ravenswood Batholith.||||||
23961|Seventy Mile Range Group|63154|5|Briefly described|p285 Fig. 5|Early Ordovician|Late Cambrian|Geological province: Charters Towers Province.||||||
23961|Seventy Mile Range Group|63600|6|Mentioned|p919|||In Charters Towers area.||||||07-FEB-11
23961|Seventy Mile Range Group|64850|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Includes Mount Windsor Volcanics, and Trooper Creek and Rollston Range Formations.||||||
23961|Seventy Mile Range Group|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Includes Mount Windsor Volcanics, and Trooper Creek and Rollston Range Formations.||||||
23961|Seventy Mile Range Group|65380|6|Mentioned|p678, p677 Fig.9|Early Ordovician|Late Cambrian|Metamorphosed in the Delamarian. Detrital zircons suggest deposition was ~500-600 Ma (Neoproterozoic).|500 - 470 Ma.|||||27-MAR-12
23961|Seventy Mile Range Group|65706|6|Mentioned|p10, p13 Tbl.1,|Early Ordovician|Late Cambrian||||Includes Mount Windsor Volcanics.||Sedimentary and felsic to intermediate volcanic rocks.|
23961|Seventy Mile Range Group|67455|4|Described|p573, p576, pp584-586, pp592-593.|Early Ordovician|Late Cambrian|Charters Towers Province. Equivalent to the metamorphosed silicic volcanic and sedimentary rocks of the Georgetown Inlier (Greenvale Province). Developed in an extensional backarc. Is younger than the Oasis Metamorphics, and overlaps the Lynwater Complex in age.|||||Lower part contains mafic dykes, sills and volcanic rocks with an intraplate/rift geochemical signature; upper part has voluminous volcanic units with a subduction-related signature, formed in an extensional backarc setting.|
23961|Seventy Mile Range Group|68307|5|Briefly described|p78, p89-91|Early Devonian|Late Cambrian|Charters Towers Province, Thomson Orogen. A S-dipping (~40 degrees), conformable succession cut by the 2km-wide Policeman Fault Zone.||||||
23961|Seventy Mile Range Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Ordovician|Cambrian|Mount Windsor Subprovince. This unit, as well as Kirk River beds and Les Jumelles beds, are all mapped under the symbol, -COs.||||||
23961|Seventy Mile Range Group|68576|5|Briefly described|Q_11: p33|||Charters Towers Province. Hosts significant VHMS deposits.||||Correlated with Balcooma Metavolcanic Group.||
23961|Seventy Mile Range Group|68679|6|Mentioned|p364|Early Ordovician|Cambrian|||||||
23961|Seventy Mile Range Group|68731|5|Briefly described|p128, p145, p146, p151, p152, p220|Early Ordovician|Early Ordovician|Charters Towers Province. Henderson (1986). At least 14 km thick in the east, thinning to the west. Deposition occurred in a continental-floored, backarc basin. Broadly correlative with the Balcooma Metavolcanics.|~ 480 Ma||Includes the Puddler Creek Formation (base), Mount Windsor Volcanics, Trooper Creek Formation, and Rollston Range Formation (top).|Correlative of the Balcooma Metavolcanic Group.|Comprises a conformable succession of sublabile to labile clastic sedimentary rocks, intermediate to felsic lavas and fragmental volcanic rocks.|
23961|Seventy Mile Range Group|68822|6|Mentioned|p320 Fig.3, p336 Fig.11, p355|Early Ordovician|Early Ordovician|Fore arc to infant arc. Charters Towers Province, Thompson Orogen.||||||
23961|Seventy Mile Range Group|68900|4|Described|p1, p4-p5, p11-p15, p18, p39|Ordovician|Cambrian|Thalanga Province. Rocks of this group were previously included in the Cape River beds in Wyatt et al, 1971). Withnall et al (1980) indicated that the Cape River Metamorphics should be restricted in area and thus rocks reassigned to the Seventy Mile Range Group by Henderson (1986).|||Includes the Kirk River beds, Les Jumelles beds, Trooper Creek Formation, Rollston Range Formation and Mount Windsor Volcanics.|||
23961|Seventy Mile Range Group|68901|6|Mentioned|p2 Fig. i|Early Ordovician|Cambrian|Thomson Orogen.||||||27-SEP-18
23961|Seventy Mile Range Group|69592|5|Briefly described|p293|||Ravenswood Batholith, Charters Towers Province.||||Is intruded by the Brittania Supersuite.||
23961|Seventy Mile Range Group|69789|5|Briefly described|p1052-1053|||S of Charters Towers. Likely source of volcanilithic sediments in Campaspe Formation.|||||Includes felsic volcanics.|
23961|Seventy Mile Range Group|69952|5|Briefly described|p4, p108|Early Ordovician|Cambrian|Charters Towers Province. Age range from graptolite fauna.|||Includes Puddler Creek Formation and Mount Windsor Volcanics.|||
23961|Seventy Mile Range Group|70033|5|Briefly described|p4|||Thomson Orogen.|||Puddler Creek Formation.|||
23961|Seventy Mile Range Group|70207|5|Briefly described|p1, p38, p42|||Charters Towers Province, Thomson Orogen. Graptolites towards the top of the unit may be Darriwilian (~469 Ma).|||Windsor Volcanics.|||
23961|Seventy Mile Range Group|70740|5|Briefly described|p1, p2, p36-p38|Early Ordovician|Late Cambrian|Drummond Basin, Mount Windsor Sub-province. May have been deposited in a deep-water environment. See also p39, p41, p80, p124, p127.|||Includes the Mount Windsor Volcanics, Puddler Creek Formation.|Intruded by the Morer Granite. Possible correlative of the Les Jumelles beds.||
23961|Seventy Mile Range Group|70744|5|Briefly described|p939, p946-947, p949-950|Early Ordovician|Late Cambrian|Charters Towers Province. Over 14 km of fill in a large-scale rift related to a back-arc extensional setting. Deposition post-dated Delamerian contraction. Fossil ages by Henderson (1983, 1986), supported by U-Pb age of 479 +/- 5 Ma (Perkins, 1995) from upper part of the unit. Base is stoped out (intruded) by granitoids of the Ravenswood Batholith.|c.488-470 Ma (estimated from Fig.7).||||A lower thick, unfossiliferous sedimentary succession overlain by a volcanic and sedimentary succession.|
23961|Seventy Mile Range Group|70749|5|Briefly described|p42-43, p54|Ordovician|Cambrian|Charters Towers Province. |~499 Ma (maximum depositional age).||Mount Windsor Volcanics.||Mainly felsic metavolcanic and metasedimentary sequences representing back arc basin deposits.|
23961|Seventy Mile Range Group|71966|5|Briefly described|p989-990,999|Ordovician|Cambrian|Geological province: Charters Towers Province, Thomson Orogen. Extensive volcanic and intrusive silicic magmatism associated with the 490-460 Ma Larapinta extensional event. Hosts significant Cu-Pb-Zn-Au-Ag bearing volcanic massive sulfide style deposits. Geochronological ages include SHRIMP U-Pb age of 479+\-5 Ma (Perkins, McDougall, & Walshe, 1993).||||||
23961|Seventy Mile Range Group|72297|5|Briefly described|p718|Early Ordovician|Late Cambrian|Hosts the tabular, blanket-like Zn deposit at Thalanga near Charters Towers.|||||Rhyolitic, dacitic and andesitic volcanic rocks.|
23961|Seventy Mile Range Group|73425|5|Briefly described|p16, 18|Early Ordovician|Early Ordovician|Charters Towers Province, northeast Thomson Orogen. Continental back-arc basin with volcaniclastic infill from the arc.|||Mount Windsor Volcanics.|||
23961|Seventy Mile Range Group|73600|6|Mentioned|p203|||Charters Towers Province. Characterised by the Pacific-Gondwanan detrital zircon ages.||||||
37961|Shadow Group|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Includes Octy, Neutral Junction, Mount Baldwin Formations and the Adam Shale.  Geological Province: southern Georgina Basin.||||||
37961|Shadow Group|62983|5|Briefly described|p11|Early Cambrian|Early Cambrian|Referred to informally as the lower Shadow Group. Siliciclastic sedimentation. Thickness: ~360m. Geological Province: Georgina Basin.||||||07-FEB-08
37961|Shadow Group|64068|3|Fully described|p224 App 1, pp54-57, p7, 36, p ix|Middle Cambrian|Neoproterozoic|New name. Includes all Lower Cambrian rocks in southern Georgina Basin. Complex relationships detailed.|||Includes Octy, Neutral Junction, Mount Baldwin and Riversdale Formations, Sylvester Sandstone, Mount Birnie beds, Adam Shale and Red Heart Dolostone.|||09-FEB-16
37961|Shadow Group|65341|6|Mentioned|p5, pp17-18.||||||Includes Octy Formation.|||
37961|Shadow Group|67323|6|Mentioned|GIS attrib tbl, Solid Geology Map.||||||Includes Mount Birnie beds, Riversdale Formation, Sylvester Sandstone|||
37961|Shadow Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
37961|Shadow Group|69377|5|Briefly described|map legend|Cambrian|Cambrian||||Mount Birnie beds|||
37961|Shadow Group|69437|6|Mentioned|p22:9|Early Cambrian|Early Cambrian|Georgina Basin, Centralian B Superbasin.||||||12-JUL-16
37961|Shadow Group|69443|5|Briefly described|p28:3, 5, 7, 13-16, 31|Cambrian|Cambrian|Kruse in Dunster et al. (2007). Includes all early Cambrian strata of the southern Georgina Basin. Represents a renewal of sedimentation following the Huckitta Movement. Is correlated with the upper Arumbera Sandstone, Winnall beds, Quandong Conglomerate, Eninta Sandstone, Mount Currie Conglomerate, Mutitjulu Arkose, Namatjira Formation and Todd River Dolostone (Amadeus Basin), and with upper Yuendumu Sandstone (Ngalia Basin).|||Neutral Junction, Octy, Mount Baldwin, Riversdale Formations; Adam Shale; Red Heart Dolostone; Sylvester Sandstone; Mount Birnie beds.|Unconformably or disconformably overlies Mopunga and Keepera Groups. Is overlain unconformably by Thorntonia Limestone, Beetle Creek or Chabalowe Formations. Correlative of Barkly Group.||12-JUL-16
37961|Shadow Group|69591|5|Briefly described|p29, p90-91, p94|Cambrian|Neoproterozoic|Oban Sub-basin, Georgina Basin.|||Riversdale Formation, Mount Birnie beds, Yardida Tillite, Black Stump Arkose, Gnallan-a-Gea Arkose.|||
37961|Shadow Group|69673|6|Mentioned|p111, p114 fig 92, p116|Cambrian|Cambrian ||||Includes Adam Shale, Mount Baldwin Formation, Octy Formation, Neutral Junction Formation, Red Heart Dolostone|||
37961|Shadow Group|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Red Heart Dolostone and the Mount Baldwin Formation.|Disconformably overlain by the Narpa Group. Unconformably overlies the Mopunga Group.||
37961|Shadow Group|72516|6|Mentioned|p12, p21, p85, p90, p135, p171, p176|Cambrian|Cambrian|Georgina Basin.|||Includes the Red Heart Dolostone, Mount Baldwin Formation|||02-JUN-21
37961|Shadow Group|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.|||Includes Mount Birnie beds.|Underlies Narpa Group.||
37961|Shadow Group|72684|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).|||Includes Mount Birnie beds|Shown as unconformably underlying Narpa Group.|Includes massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
37961|Shadow Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
37961|Shadow Group|73137|6|Mentioned|p6|Cambrian|Cambrian|||||||
37961|Shadow Group|73553|6|Mentioned|p7|Cambrian|Cambrian|||||||
36265|Shady Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36265|Shady Microgranite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|||||||
36265|Shady Microgranite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Included in Nettle Granite on most recent maps. Topaz-bearing microgranite. I-type.||||||07-FEB-11
23963|Shamrock Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Kungaree Volcanic Subgroup. Thickness: Up to 250m. Geological Province: Georgetown Region.||||||28-MAY-15
23963|Shamrock Rhyolite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Kungaree Volcanic Subgroup, Newcastle Range Volcanic Group.||||||
23963|Shamrock Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V19. Assumed to be I-Type.||||||
23963|Shamrock Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23963|Shamrock Rhyolite|40542|6|Mentioned|p97|||||||||
23963|Shamrock Rhyolite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Kungaree Volcanic Subgroup.||||||
23963|Shamrock Rhyolite|43740|4|Described|p8|||||||||
23963|Shamrock Rhyolite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Kungaree Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
23963|Shamrock Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Kungaree Volcanic Subgroup.|||Grey to brown or purple crystal-rich rhyolitic ignimbrite; lesser green to brown and purple rhyolitic volcanic lutite to volcanic arenite.|
75648|Shannon Vale Gabbro|68679|5|Briefly described|p366 Fig.5.55||||||||Pegmatoidal gabbro containing numerous black elongate hornblende grains to 8cm long set in mostly pale grey plagioclase.|
75648|Shannon Vale Gabbro|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Dark grey, fine to medium-grained, uneven-grained to moderately porphyritic (olivine-orthopyroxene-clinpopyroxene) hornblende gabbro; minor very coarse (pegmatitic) hornblende gabbro (`hornblendite').|
35033|Shawlands Granite Complex|23037|6|Mentioned|p76|||Misspelt Shawlands Granodiorite Complex? .||||||10-SEP-19
35033|Shawlands Granite Complex|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgsl].  Pale grey to pinkish-grey, medium-grained granite to monzonite; grey to white, medium-grained hornblende-biotite granodiorite to diorite, minor potassic alteration.||||||
35033|Shawlands Granite Complex|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Hornblende-biotite granite to monzonite; hornblende-biotite granodiorite to diorite.||||||18-MAY-04
35033|Shawlands Granite Complex|65388|2|Defined|p275, p236 Fig. 81, p237, 238, 254, 263|Early Permian|Carboniferous|Relationships masked by poor outcrop. May intrude Tindarra Granite, but may be related to mid-Carboniferous Glendore Granodiorite. Relationship with Glenhalvern Granite [and Lonesome Creek Quartz Monzodiorite] is unclear. Age uncertain. Magma mingling compared with Kooingal Granodiorite Complex. A range of granitoid types including light grey to pinkish-grey medium-grained granite to monzonite and grey to white, medium-grained hornblende-biotite granodiorite to diorite or possibly monzonite.||||||
35033|Shawlands Granite Complex|68679|5|Briefly described|p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age uncertain. Contacts masked by poor outcrop. See also reference to Shawlands Granodiorite Complex (p408).|||||Range of rocks: grey to pinkish grey, medium-grained granite to monzonite; grey to white, medium-grained hornblende-biotite granodiorite to diorite; zone of magma mixing where granodiorite-diorite-monzonite contain enclaves of fine-grained diorite.|
29332|Sheba Granite|23291|5|Briefly described|p103 Tb. 3.13|Late Carboniferous|Late Carboniferous|May be intruded by Kitchener Granite and Martin Creek Microgranite? Geological Province: Georgetown Region.||||||30-MAR-15
29332|Sheba Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
29332|Sheba Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29332|Sheba Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
29332|Sheba Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 323. I-Type.||||||
29332|Sheba Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29332|Sheba Granite|43083|5|Briefly described|p256|||Of Ootann Supersuite. Intrudes Chillagoe Formation; inferred to cut part of Reddicliffe Granite. I-type.  Lithology included.||||||17-JUN-09
29332|Sheba Granite|43087|2|Defined|p43|Late Carboniferous||Of Ootann Supersuite.||||||02-JUN-09
29332|Sheba Granite|43259|4|Described|Appendix 1,p39.||Carboniferous|||||||
29332|Sheba Granite|60425|4|Described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. I-type. Pink, fine- to medium-grained, slightly to highly porphyritic biotite granite; leucocratic; rare hornblende, titanite.||||||07-FEB-11
29332|Sheba Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, slightly to highly porphyritic biotite syenogranite and monzogranite.|
29332|Sheba Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink, medium-grained, slightly to highly porphyritic biotite syenogranite and monzogranite.|
29332|Sheba Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink to pale pinkish grey, fine- to medium-grained, moderately to highly porphyritic biotite monzogranite; with scattered inclusions of "diorite" (up to ~10 cm), biotite granodiorite (to ~50 cm) and quartz (rare; to ~15 cm).|
27653|Shield Creek Formation|23032|4|Described|p24,25 fig6||Early Devonian|||||||
27653|Shield Creek Formation|23424|5|Briefly described|Table 8.1 Fig 8.3 p334.|Pragian|Lochkovian|Graveyard Creek Subprovince.||||||
27653|Shield Creek Formation|23430|4|Described|p479, p505-506|||Upper and lower. Also see p479 and Plate 14.11. Overlying Unit Broken River Group - unconformable. Graveyard Creek Subprovince.||||||
27653|Shield Creek Formation|23431|5|Briefly described|p541|||||||||
27653|Shield Creek Formation|23522|5|Briefly described|p250 Fig 6|Pragian|Lochkovian|||||||
27653|Shield Creek Formation|23617|6|Mentioned|p47|||Broken River Province.||||||
27653|Shield Creek Formation|23893|5|Briefly described|p9 Fig. 4|Middle Devonian|Early Devonian|||||||
27653|Shield Creek Formation|24577|5|Briefly described|p752 Fig. 1|Emsian|Lochkovian|Overlies the Ralph Flint Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
27653|Shield Creek Formation|24612|5|Briefly described|p12|Early Devonian|Early Devonian|Contains Carlinastraea fauna.||||||06-APR-05
27653|Shield Creek Formation|24613|5|Briefly described|p6 Fig. 3|Middle Devonian|Early Devonian|Geological province: Burdekin Basin.||||||07-FEB-11
27653|Shield Creek Formation|24614|5|Briefly described|p191 Fig. 1, p206|||Contains the Arch Creek and Martins Well limestone members. Geological Province: Broken River Province.||||||07-FEB-11
27653|Shield Creek Formation|37573|6|Mentioned|p202|||See also Fig.2||||||
27653|Shield Creek Formation|37768|5|Briefly described|p41|||||||||
27653|Shield Creek Formation|38658|6|Mentioned|p152|||||||||
27653|Shield Creek Formation|39445|5|Briefly described|Table 5|||See also P71 & P74||||||
27653|Shield Creek Formation|41260|3|Fully described|p47|||See also P159 and Fig.18||||||
27653|Shield Creek Formation|41675|6|Mentioned|p94|||||||||
27653|Shield Creek Formation|41679|2|Defined|p252|Emsian||||||||
27653|Shield Creek Formation|41719|6|Mentioned|p213|||||||||
27653|Shield Creek Formation|41739|6|Mentioned|p299|||See also Fig.2||||||
27653|Shield Creek Formation|42031|5|Briefly described|p760|||||||||
27653|Shield Creek Formation|42032|5|Briefly described|p494|||||||||
27653|Shield Creek Formation|42054|6|Mentioned|p273|||||||||
27653|Shield Creek Formation|42279|6|Mentioned|Fig.2 P18|||||||||
27653|Shield Creek Formation|42581|5|Briefly described|Fig 1. P36|||||||||
27653|Shield Creek Formation|42692|5|Briefly described|map legend|Devonian||||||||
27653|Shield Creek Formation|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
27653|Shield Creek Formation|42709|6|Mentioned|map legend|||||||||
27653|Shield Creek Formation|42752|5|Briefly described|p47|||see also Fig.3 P47||||||
27653|Shield Creek Formation|42933|2|Defined|p74|Early Devonian||Of Graveyard Creek Group.||||||04-FEB-08
27653|Shield Creek Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|No longer included in Graveyard Creek Group. Conodonts indicate younger age.||||||
27653|Shield Creek Formation|44447|6|Mentioned|p135|Early Devonian|Early Devonian|Includes Martin's Well Limestone Member and Arch Creek Limestone Member.||||||
27653|Shield Creek Formation|50088|6|Mentioned|p469|||Includes Martins Well Limestone Member. Contains conodonts.||||||24-FEB-05
27653|Shield Creek Formation|50093|5|Briefly described|p329 Fig.2|Pragian|Lochkovian|||||||07-FEB-11
27653|Shield Creek Formation|61211|5|Briefly described|p275 Fig. 16|Early Devonian|Late Silurian|Geological Province: Broken River Province.||||||13-JAN-06
27653|Shield Creek Formation|61727|5|Briefly described|p942 Fig.1|Devonian|Devonian|Geological Province: Broken River Province/Camel Creek Subprovince.||||||
27653|Shield Creek Formation|63152|5|Briefly described|p120 Fig. 3|Pragian|Lochkovian|Feldspathic and quartzose arenites with three areally isolated limestone members.||||||
27653|Shield Creek Formation|63154|5|Briefly described|p281 Fig. 3|Early Devonian|Early Devonian|Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
27653|Shield Creek Formation|65214|6|Mentioned|p272, p275|Devonian|Devonian|QLD, Broken River and North. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27653|Shield Creek Formation|65940|6|Mentioned|p203|Pragian|Pragian|Contains A. kennediense (see Yu and Jell, 1990).||||||
27653|Shield Creek Formation|66498|6|Mentioned|p43|Pragian|Early Devonian||||Martins Well Limestone Member.|||
27653|Shield Creek Formation|68336|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Martins Well Limestone Member.||Coarse-grained, feldspathic to quartzose sandstone and local conglomerate; minor fine-grained sandstone, siltstone and mudstone; local limestone.|
27653|Shield Creek Formation|68341|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.|||Includes Martins Well Limestone Member.||Coarse-grained, feldspathic to quartzose sandstone and local conglomerate; minor fine-grained sandstone, siltstone and mudstone; local limestone.|
27653|Shield Creek Formation|68478|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.|||||Coarse-grained, feldspathic to quartzose sandstone and local conglomerate; minor fine-grained sandstone, siltstone and mudstone; local limestone.|
27653|Shield Creek Formation|68479|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Graveyard Creek Subprovince.|||||Coarse-grained, feldspathic to quartzose sandstone and local conglomerate; minor fine-grained sandstone, siltstone and mudstone; local limestone.|
27653|Shield Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Broken River Province. This unit, as well as the Blue Rock Creek beds, Conjuboy Formation and Broken River Group, are all mapped under the symbol, Db.||||||
27653|Shield Creek Formation|69030|5|Briefly described|p6|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province).|||Arch Creek, Martins Well, Limestone Members.|||
27653|Shield Creek Formation|69079|6|Mentioned|p5|Early Devonian|Early Silurian|Graveyard Creek Subprovince, Broken River Province.||||||
27653|Shield Creek Formation|69592|3|Fully described|p259-261, p263-264, p266-267, p301, p303|Early Devonian|Silurian|Graveyard Creek Subprovince, Broken River Province. Widely distributed. Up to 850m thick, thinning southwards to just a few metres. Fence diagram. Previously excluded from Graveyard Creek Group and Broken River Group by Lang et al. (1989) and Withnall et al. (1993); here included in the former because of its gradational relationship with the Quinton Formation. Has a composite type section (Withnall et al., 1998; Lang et al., 1989; Withnall et al., 1993) near the core of the Atherton Creek Anticlinorium. Lithologies and fossils described in some detail. Coastal plain to inner shelf deposits. Age also given as Pragian.||Graveyard Creek Group.|Martins Well, Arch Creek, Limestone Members.|Conformably overlies Quinton, Ralph Flint and Jack Formations. Is overlain by Bracteata Mudstone (Broken River Group).|Lower interval of coarse- to very coarse-grained feldspathic sandstone, quartzose sandstone and minor conglomerate; then finer sandstone, siltstone and mudstone to the limestone Member; up to feldspathic sandstone with calcareous mudstone interbeds.|
27653|Shield Creek Formation|73143|6|Mentioned|p17|Pragian|Pragian|Broken River Province. Contains rugose coral, Cystiphylloides sp. A (Yu and Jell, 1990).||||||
27653|Shield Creek Formation|73201|5|Briefly described|p612-315, p617-618|Pragian|Lochkovian|Graveyard Creek Province [Subprovince?]. From the forearc basin adjacent to the Broken River subduction complex. Geochron is a U-Pb LA-ICP-MS detrital zircon maximum depositional age and is consistent with biostratigraphic constraint for limestone intervals. Detrital zircon age distribution matches that of the Greenvale Formation, Perry Creek Formation, and especially the Kangaroo Hills Formation, which show provenance linkages to igneous rocks of the Macrossan and Pama Igneous associations. Significantly, no Proterozoic grain ages show in the analyses in spite of close proximity to the North Australian Craton.|411.5 +/- 5.5 Ma||||Includes arkose.|
75148|Shiptons Flat Supersuite|60425|6|Mentioned|p93 Fig. 29, p95|||Includes microgranite/rhyolite dykes in northeastern Cairns region. S-type granites.||||||07-FEB-11
22844|Shovel Creek Complex|23049|4|Described|p11|||||||||
22844|Shovel Creek Complex|23283|2|Defined|p25|Devonian|Silurian|||||||
22844|Shovel Creek Complex|23422|5|Briefly described|p212 Table 6.7|||||||||
22844|Shovel Creek Complex|23505|5|Briefly described|Map legend|Devonian|Ordovician|||||||
22844|Shovel Creek Complex|68553|6|Mentioned|Map legend|Ordovician|Cambrian|Charters Towers Province. This unit and the Fat Hen Creek Complex are mapped under the same symbol, -COgm.||||||
26894|Shrimp Creek Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Age: 330Ma (Black & Holmes, unpub.ms.). Thickness: 500-600m. Geological Province: Georgetown Region.||||||08-JUL-15
26894|Shrimp Creek Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V24. I-Type.||||||
26894|Shrimp Creek Rhyolite|23619|4|Described|p31 Table 1||Carboniferous|Of Eveleigh Volcanic Subgroup, of Newcastle Range Volcanic Group. Underlying Unit Mosaic Gully Rhyolite.||||||
26894|Shrimp Creek Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
26894|Shrimp Creek Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
26894|Shrimp Creek Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Eveleigh Volcanic Subgroup||||||
26894|Shrimp Creek Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
26894|Shrimp Creek Rhyolite|43740|5|Briefly described|p13|||||||||
26894|Shrimp Creek Rhyolite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Of the Newcastle Range Volcanic Group).||||||
26894|Shrimp Creek Rhyolite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Ignimbrite. Of the Eveleigh Volcanic Subgroup.||||||19-AUG-04
26894|Shrimp Creek Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|||Grey to brown crystal-rich rhyolitic ignimbrite containing variable amounts of hornblende and biotite; locally lithic-rich.|
26894|Shrimp Creek Rhyolite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.||Of the Eveleigh Volcanic Subgroup.|||Grey to brown crystal-rich rhyolitic ignimbrite containing variable amounts of hornblende and biotite; locally lithic-rich.|
75149|Siding granite|60425|6|Mentioned|p49 Tb.3|||Intruded Boonmoo Volcanic Subgroup.||||||07-FEB-11
36302|Silent Creek Volcanic Group|23291|4|Described|p42, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
36302|Silent Creek Volcanic Group|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
36302|Silent Creek Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Elimeek and Wallaman Falls Volcanics; Janet Ranges, Koolmoon and Torres Strait Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
36302|Silent Creek Volcanic Group|69593|6|Mentioned|p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
30201|Silent Hill Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Parent: McBride Basalt Group. Age: 0.89Ma. Geological Province: Georgetown Region.||||||08-JUL-15
30201|Silent Hill Basalt|23619|4|Described|p28 table 1||Pleistocene|Of the McBride Basalt Group in the McBride Basalt Province.||||||
30201|Silent Hill Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
30201|Silent Hill Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
30201|Silent Hill Basalt|68576|5|Briefly described|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
30201|Silent Hill Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pleistocene|Pleistocene|McBride Basalt Province.|0.37 Ma|||||
25477|Silver Hills Volcanics|22557|6|Mentioned|p569|||||||||
25477|Silver Hills Volcanics|22604|5|Briefly described|p438, Fig.2 p439||Late Devonian|||||||
25477|Silver Hills Volcanics|22675|4|Described|p172 App.3|Early Carboniferous|Late Devonian|Drummond Basin||||||
25477|Silver Hills Volcanics|22800|3|Fully described|Fig.14 p592, p580|Tournaisian|Tournaisian|U-Pb zircon age 344 Ma (SHRIMP). See also p584, p589, p591||||||
25477|Silver Hills Volcanics|23052|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
25477|Silver Hills Volcanics|23161|4|Described|p9 table 2a|Early Carboniferous|Late Devonian|Ages: 351.2+/-4Ma to 357.4+/-3.3Ma.||||||
25477|Silver Hills Volcanics|23430|5|Briefly described|p491 & p510|||Drummond Basin Province.||||||
25477|Silver Hills Volcanics|23854|5|Briefly described|p859 Fig 3|Devonian|Devonian|||||||
25477|Silver Hills Volcanics|23986|6|Mentioned|p102|||||||||
25477|Silver Hills Volcanics|23988|5|Briefly described|p50|||See also page 52.||||||
25477|Silver Hills Volcanics|24031|5|Briefly described|p2, p3 Fig. 1, p15 Tb. 4, p29-31|Carboniferous|Carboniferous|Overlain unconformably by Suttor Formation. Comprises quartz latite ignimbrites.||||||
25477|Silver Hills Volcanics|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Late Devonian|Rhyolite, trachyte, andestite and tuff; minor lithic sandstone and mudstone.  Max. thickness: 1500m.  Geological Province: Drummond Basin.||||||
25477|Silver Hills Volcanics|24424|5|Briefly described|p539 Tb.4|Carboniferous|Devonian|Age: 320-370 Ma. Palaeomagnetic poles given. Geological Province: Drummond Basin.||||||04-FEB-05
25477|Silver Hills Volcanics|30102|6|Mentioned|p4|||Pre-Permian age.||||||
25477|Silver Hills Volcanics|30691|4|Described|p12|||See also P21,Table 3. Upper Devonian-Lower Carboniferous||||||
25477|Silver Hills Volcanics|30814|2|Defined|p66|Late Devonian|Late Devonian|||||||
25477|Silver Hills Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
25477|Silver Hills Volcanics|31999|5|Briefly described|p136|||Table 1||||||
25477|Silver Hills Volcanics|32490|4|Described|Table 1|||U.Dev.-L.Carb.||||||
25477|Silver Hills Volcanics|32493|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|U.Dev.-L.Carb.||||||
25477|Silver Hills Volcanics|32865|4|Described|p483|||Late Dev. - early Carb.||||||
25477|Silver Hills Volcanics|33078|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25477|Silver Hills Volcanics|33079|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25477|Silver Hills Volcanics|33086|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian to Lower Carboniferous||||||
25477|Silver Hills Volcanics|33092|4|Described|p5|||Strat. table P7.||||||
25477|Silver Hills Volcanics|33096|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
25477|Silver Hills Volcanics|33641|6|Mentioned|p59|||U.Dev.||||||
25477|Silver Hills Volcanics|33646|6|Mentioned|p7|||Late Dev.||||||
25477|Silver Hills Volcanics|34174|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25477|Silver Hills Volcanics|34389|4|Described|Table 1|||Upper Devonian||||||
25477|Silver Hills Volcanics|34390|4|Described|Table 1|||Upper Devonian||||||
25477|Silver Hills Volcanics|34391|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25477|Silver Hills Volcanics|34392|6|Mentioned|Map legend|Late Devonian|Late Devonian|Upper Devonian - Lower Carboniferous||||||
25477|Silver Hills Volcanics|34408|6|Mentioned|p185|||On table||||||
25477|Silver Hills Volcanics|37451|6|Mentioned|Table 2|||||||||
25477|Silver Hills Volcanics|37565|6|Mentioned|Fig.8|||||||||
25477|Silver Hills Volcanics|37573|5|Briefly described|Table 2|||||||||
25477|Silver Hills Volcanics|37613|6|Mentioned|p249|||See also Fig.3||||||
25477|Silver Hills Volcanics|38527|6|Mentioned|p303|||||||||
25477|Silver Hills Volcanics|39445|5|Briefly described|Table 6|||||||||
25477|Silver Hills Volcanics|40623|5|Briefly described|p80|||||||||
25477|Silver Hills Volcanics|40685|5|Briefly described|p400|||||||||
25477|Silver Hills Volcanics|41246|6|Mentioned|Map legend|Devonian||||||||
25477|Silver Hills Volcanics|41272|5|Briefly described|M 1of1 K11|||||||||
25477|Silver Hills Volcanics|41825|6|Mentioned|p205|||||||||
25477|Silver Hills Volcanics|42486|5|Briefly described|p201|||||||||
25477|Silver Hills Volcanics|42547|5|Briefly described|p60|||||||||
25477|Silver Hills Volcanics|42614|4|Described|p9|||Drummond Basin||||||
25477|Silver Hills Volcanics|42678|6|Mentioned|p246|||||||||
25477|Silver Hills Volcanics|42701|3|Fully described|p20|||||||||
25477|Silver Hills Volcanics|42747|5|Briefly described|p39, Fig.10|||subdivided into about 40 different units||||||
25477|Silver Hills Volcanics|43029|5|Briefly described|Fig.1,p13|||||||||
25477|Silver Hills Volcanics|43099|4|Described|p8|||||||||
25477|Silver Hills Volcanics|43105|6|Mentioned|p11|||||||||
25477|Silver Hills Volcanics|43204|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||underlies Telemon Formation||23-DEC-11
25477|Silver Hills Volcanics|43213|2|Defined|p10-11, p16-17, p21, p67, p75-91, p117|Early Carboniferous|Late Devonian|See also p125-129, p193, p227-229, p238, p241, p245. Webb et al. (1963); described by Veevers et al. (1964), and Olgers (1972) who designated a type area in Spring Creek (details of this and measured sections are given). Named after Silver Hills homestead. Occurs as scattered outcrops in, and overlies W edge of, Anakie Inlier; forms basal part of the Drummond Basin sequence. Here subdivided into about 40 different units in 5 areas: detailed lithologies for each unit are described. Is faulted against Rolfe Creek Schist. Very few fossils: Leptophloeum australe. Potential for epithermal Au deposits. Geophysics, chemical analyses detailed.||||Unconformably overlies Taroborah Granodiorite, Anakie Metamorphic Group and Theresa Creek Volcanics, and Greybank Volcanics conformably.  Underlies Telemon Formation disconformably.|Continental felsic volcanic assemblage: rhyolitic ignimbrites, rhyolitic lavas, dacitic to trachyandesitic lavas, epiclastic and basement-derived sedimentary rocks.|
25477|Silver Hills Volcanics|43461|14|Not recorded|p616, Table p618|||U/C on Dunstable Formation||||||
25477|Silver Hills Volcanics|43861|5|Briefly described|24; Fig1 p26; 29|Early Carboniferous|Late Devonian|||||||
25477|Silver Hills Volcanics|43990|14|Not recorded|Map Legend||Late Devonian|||||||
25477|Silver Hills Volcanics|43994|14|Not recorded|Map Legend|||||||||
25477|Silver Hills Volcanics|43998|4|Described|p20,map|Carboniferous|Devonian|||||||
25477|Silver Hills Volcanics|43999|14|Not recorded|p95,96|||||||||
25477|Silver Hills Volcanics|44081|14|Not recorded|p31,45,48,59,61-4,73|||p75-6,90,111,114,160,206-7,Pl.1-4,6. Described in French.||||||
25477|Silver Hills Volcanics|44124|14|Not recorded|p6|Carboniferous|Devonian|||||||
25477|Silver Hills Volcanics|44245|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
25477|Silver Hills Volcanics|44331|14|Not recorded|Map Legend|Early Carboniferous|Late Devonian|||||||
25477|Silver Hills Volcanics|44337|5|Briefly described|Map Legend||Late Devonian|Lithology.||||||
25477|Silver Hills Volcanics|45071|3|Fully described|Table 1|||||||||
25477|Silver Hills Volcanics|45073|6|Mentioned|p26|||Refers Veerers et al. (1964b). Strat. p14.||||||
25477|Silver Hills Volcanics|45097|6|Mentioned|Fig.|||Correlation chart||||||
25477|Silver Hills Volcanics|46849|6|Mentioned|Fig. 2|||||||||
25477|Silver Hills Volcanics|46881|6|Mentioned|p195|||||||||
25477|Silver Hills Volcanics|48843|14|Not recorded|p.8,14,16,17,map|Carboniferous|Devonian|(F55-11).||||||
25477|Silver Hills Volcanics|48845|2|Defined|p6-8,10-19,23-7,map.||Late Devonian|Fig.10. Upper Devonian or older.  Dominantly acid volcanic complex west of Anakie Inlier, previously identified as Dunstable Formation. Overlies Anakie Metamorphics and Retreat Granite. Underlies Telemon Formation.||||||
25477|Silver Hills Volcanics|48900|4|Described|p11|||||||||
25477|Silver Hills Volcanics|48908|6|Mentioned|p21|Carboniferous|Devonian|||||||
25477|Silver Hills Volcanics|48920|3|Fully described|p15|||See also Table 4. Upper Devonian - Lower Carboniferous age||||||
25477|Silver Hills Volcanics|60369|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Overlain by the Telemon Formation. Flow banded and spherulitic rhyolite, agglomerate, tuff, minor sediments.||||||02-SEP-04
25477|Silver Hills Volcanics|60659|5|Briefly described|p12, p75, p85|Early Carboniferous|Late Devonian|Complex of rhyolitic to dacitic volcanic facies. Age: 351.2+/-4.0Ma to 357.4+/-3.3Ma. Geological Province: Drummond Basin.||||||07-FEB-11
25477|Silver Hills Volcanics|60705|5|Briefly described|p650|Early Carboniferous|Late Devonian|Rhyolitic volcanics. Geological Province: Drummond Basin. Age: 347+/-2.9 Ma and 357.4+/-3.3 Ma.||||||12-APR-05
25477|Silver Hills Volcanics|61777|5|Briefly described|p229|Early Carboniferous|Late Devonian|Age: ca 344Ma (Henderson et al., 1998). Geological Province: Drummond Basin.||||||07-FEB-11
25477|Silver Hills Volcanics|64315|5|Briefly described|p510 Tb. 1|Early Carboniferous|Late Devonian|Max. thickness: 1500m. Geological province: southern Drummond Basin. Rhyolite, trachyte, andesite, tuff; minor lithic sandstone, mudstone.||||||
25477|Silver Hills Volcanics|64855|5|Briefly described|p25, 26|Early Carboniferous|Late Devonian|Crop out along the western edge of the Anakie Inlier. Form base of Drummond Basin. Seismic interp. suggests up to 3 km thick. Rhyolitic ignimbrites encountered in exploration wells west of the Drummond Basin are correlated with this formation.||||||22-FEB-10
25477|Silver Hills Volcanics|65388|6|Mentioned|p189|||Unconformably overlain by Blenheim Formation on western side of Bowen Basin.||||||
25477|Silver Hills Volcanics|65668|5|Briefly described|p1, p2 Tb.1, p4-7|Carboniferous|Late Devonian|Drummond Basin, Age: 362.8 +/- 2.7 Ma (SHRIMP U-Pb zircon). Dacitic volcanics and volcaniclastics. Hosts the Glen Eva gold-silver mine near Mount Coolon; also the Lone Sister prospect ~80 km to the SW, dated 357.4 +/- 3.3 Ma (SHRIMP U-Pb zircon; Perkins et al., 1995).||||||
25477|Silver Hills Volcanics|66084|5|Briefly described|Map legend|Carboniferous|Late Devonian|Flow-banded rhyolites, rhyolitic ignimbrites, dacite, lithic tuff, microgranite, quartz diorite; minor pebble conglomerate, sandstones, siltstones.||||||
25477|Silver Hills Volcanics|66085|5|Briefly described|Map legend|Carboniferous|Devonian|Rhyolite, rhyolitic ignimbrites, dacite, lithic tuff; minor pebble conglomerate, sandstone, siltstone.||||||
25477|Silver Hills Volcanics|66086|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone and siltstone.||||||15-MAR-13
25477|Silver Hills Volcanics|66188|6|Mentioned|Fig 3|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
25477|Silver Hills Volcanics|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5||Devonian|Age shown in Fig 7 is Devonian, but numeric age is Devonian-Permian. Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|280-380 Ma magnetic age range|||||10-AUG-15
25477|Silver Hills Volcanics|67402|6|Mentioned|p196 fig DRM2, p197|Tournaisian|Famennian|Drummond Basin.||||Overlain by the Telemon Formation.||
25477|Silver Hills Volcanics|68328|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian||||||Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone and siltstone.|
25477|Silver Hills Volcanics|68329|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian||||||Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone and siltstone.|
25477|Silver Hills Volcanics|68404|5|Briefly described|Map legend|Carboniferous|Devonian|Drummond Basin|||||Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone, and siltstone.|
25477|Silver Hills Volcanics|68411|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||Conformably overlain by Mount Hall Formation or Raymond Sandstone. Unconformably underlain by the Sedgeford Formation.|Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, minor sandstone and siltstone.|18-JUN-13
25477|Silver Hills Volcanics|68412|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Drummond Basin. Nineteen individual un-named sub-units are mapped separately.|||||Rhyolites and dacites: often flow-banded, spherulitic, porphyritic, crystal or lithic rich; volcanic breccia; conglomerate, sandstone, siltstone, tuff; rare obsidian and andesite.|
25477|Silver Hills Volcanics|68482|5|Briefly described|Map Legend|Visean|Frasnian|16 unnamed facies are mapped separately. Isotopic ages have been determined from zircons within topmost unit (rhyolitic ignimbrite) using U-Pb SHRIMP geochronology. |371.2 +/- 6 Ma; 343.7 +/- 5.3 Ma||||Rhyolites, rhyolitic ignimbrite, crystal and lithic tuffs, dacite, trachyandesite, volcanic breccia; conglomerate, sandstone, breccia, siltstone.|
25477|Silver Hills Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Bimurra, Foyle and Stones Creek Volcanics, and the Mount Wyatt and Saint Anns Formations, are all mapped under the symbol, DCD1.||||||
25477|Silver Hills Volcanics|68679|5|Briefly described|p363, p372|Mississippian|Late Devonian|Drummond Basin.|362.8 +/- 2.7 Ma (SHRIMP: Cross et al., 2009)||||Rhyolite lava (Glen Eva pit).|
25477|Silver Hills Volcanics|68731|5|Briefly described|p125, p174, p191, p191 Fig 3.102|Middle Devonian|Middle Devonian|Anakie Inlier. ~ 2km thick. In the Nogoa and Telemon anticlines, volcanics previously assigned to the Silver Hills Volcanics are now mapped on NANDOWRIE as the Foyles Volcanics, distinguished by their geochemistry.|344 +/- 3 Ma, K-Ar|||Disconformably overlain by the Mount Rankin Formation.|Comprises largely silicic ignimbrite and lava. Ignimbrite commonly incorporates metamorphic clasts. Lavas are characteristically flow-banded trachydacite and rhyolite.|28-AUG-14
25477|Silver Hills Volcanics|68900|3|Fully described|p1, p4, p32, p37-p38, p49-p52, p56-p57|Early Carboniferous|Late Devonian|Drummond Basin. Originally named by Veevers & others (1964) after Silver Hills homestead in the Emerald 1:250k sheet. Crops out from midway along the eastern margin of the basin. Described in detail by Blake et al (1995). Superseded? by the Foyle Volcanics. Usually resistant to weathering and forms hilly topography. These rocks have a high K signature in airborne radiometric images and generally have a low magnetic signature. Lithology is discussed in detail. Interpreted to have erupted sub-aerially whilst the sediments were deposited in local fluvial and lacustrine environments.Between 250 and 1500m thick in measured sections. Hosts poorly preserved lycopod fossils which are the source of the assigned ages. Age equivalent to the Saint Anns Formation, Foyle Volcanics and possibly the Vera-Nancy Volcanics and Stones CreekVolcanics. Faulted against the Sedgeford Formation.||||Unconformably overlies (or is faulted against) the Anakie Metamorphic Group or Les Jumelles beds. Conformably (to disconformably) overlain by the Telemon Formation and Mount Hall Formation.|Dacitic to rhyolitic volcanics including lava flows and ignimbrite, and minor volcaniclastic siltstones and sandstones.|
25477|Silver Hills Volcanics|69379|5|Briefly described|map legend|Early Carboniferous|Late Devonian||||||Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone and siltstone|
25477|Silver Hills Volcanics|69599|6|Mentioned|p593|||||||Is overlain unconformably by Red Mountain Formation.||
25477|Silver Hills Volcanics|69952|5|Briefly described|p115|||SHRIMP U-Pb zircon age of a correlate from the Mount Coolan region.|362.8 +/- 2.7 Ma (Cross et al., 2009).|||Overlies Theresa Creek Volcanics.|Includes rhyolite.|
25477|Silver Hills Volcanics|70740|5|Briefly described|p1, p7, p8, p41, p50, p81|Late Devonian|Late Devonian|Drummond Basin. SHRIMP age derived from Cross et al, 2009, Easting and Northing for sample is provided. Another SHRIMP age of 357.4 +/- 3.3 from Perkins et al, 1995 is given. Partly equivalent to Saint Anns Formation and Stones Creek Volcanics.|362.8 +/- 2.7 (SHRIMP U-Pb)|||Equivalent to the Bimurra Volcanics and the Saint Anns Formation.|Rhyolitic to dacitic lava flows and ignimbrite, minor volcaniclastic siltstone, sandstone and sinter.|
25477|Silver Hills Volcanics|70856|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Seven facies are mapped separately.||||Is overlain unconformably by Telemon Formation.|Aphyric, spherulitic and porphyritic flow banded rhyolites, aphyric to porphyritic flow banded dacite, volcanic conglomerates, breccias and sandstone.|
25477|Silver Hills Volcanics|71592|5|Briefly described|Appendix A.|||Drummond Basin.|363+/-2.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite, ignimbrite, trachyte.|
25477|Silver Hills Volcanics|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Late Devonian|Geological province: southern Drummond Basin.||||Overlain by Telemon Formation. Equivalent to the upper part of the St Anns Formation in the northern Drummond Basin.||
25477|Silver Hills Volcanics|73035|5|Briefly described|Map legend|Early Carboniferous|Late Devonian||||||Rhyolite, dacite, rhyolitic ignimbrite, volcaniclastic sediments, sinter, minor sandstone and siltstone.|
25477|Silver Hills Volcanics|73179|6|Mentioned|p1134 Fig.1, p1143, p1152|Visean|Famennian|Drummond Basin. Geochron from Cross et al. (2008).|ca 360-340 Ma||||Dominated by rhyolitic to dacitic ignimbrites and lavas.|20-SEP-22
25477|Silver Hills Volcanics|73197|6|Mentioned|p465 Fig.4|Carboniferous|Carboniferous|Drummond Basin.|||||Volcanics.|
25477|Silver Hills Volcanics|73198|4|Described|p499-502, p507, p511-512, p514|||Drummond Basin, south. Part of Cycle 1 of Olgers (1972). Records basin-wide contemporaneous volcanism. Maximum thickness: ca 2000 m. Volcanic provenance. [See article for petrographic descriptions and data].||||Overlain by Telemon Formation. Equivalent to Saint Anns Formation.|Includes crystal-rich, feldspar-phyric, partly welded silicic ignimbrite.|
23973|Silver Plains Nephelinite|22780|5|Briefly described|map|Pliocene|Pliocene|||||||
23973|Silver Plains Nephelinite|22781|4|Described|p45|Early Pliocene|Early Pliocene|~3.72+/-0.06Ma||||||
23973|Silver Plains Nephelinite|23420|5|Briefly described|p 131|||||||||
23973|Silver Plains Nephelinite|42610|2|Defined|p32|early Pliocene||Age 3.72+/-.06Ma K/Ar.||||||
23973|Silver Plains Nephelinite|42650|6|Mentioned|p17|||||||||
23973|Silver Plains Nephelinite|43738|6|Mentioned|p51|||||||||
23973|Silver Plains Nephelinite|44872|5|Briefly described|Map Legend||Pliocene|||||||
23973|Silver Plains Nephelinite|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as the Mount Barney Central Complex, Tabor Gabbro, Mount Jukes Intrusive Complex, and unnamed basaltic to rhyolitic plugs, are all mapped under the symbol, Ti.||||||
23973|Silver Plains Nephelinite|69599|5|Briefly described|p641|Pliocene|Pliocene|58km SE of Coen. Represents a primary mantle melt; has a Mg number of 68.|3.72 +/- 0.06 Ma (Sutherland, 1991).||||Several nephelinite lava flows of one of the most silica-undersaturated volcanic rocks associated with the intraplate Eastern Australian Cainozoic Igneous Province.|
23973|Silver Plains Nephelinite|71792|5|Briefly described|p61|Pliocene|Pliocene|Overlies the Carpentaria Basin.|||||Nephelinite.|
23973|Silver Plains Nephelinite|71849|5|Briefly described|p8, p80, p195|Pliocene|Pliocene|Crops out ~50km SE of Coen.|3.72 +/- 0.06 Ma. K-Ar: Sutherland (1991).|||||
23973|Silver Plains Nephelinite|71854|5|Briefly described|Map legend.|Pliocene|Pliocene||||||Nephelinite.|
36171|Silver Pot Granodiorite|23423|4|Described|p240||Early Permian|Previously mapped as part of the Kalunga Granodiorite. Age: 276-280 Ma (Rb-Sr). Almaden Supersuite. Kennedy Igneous Province.||||||
36171|Silver Pot Granodiorite|23506|5|Briefly described|Map Legend||Early Permian|of Almaden Supersuite. Age: ~276 Ma Rb-Sr.||||||
36171|Silver Pot Granodiorite|60425|4|Described|p74, p282-3 Appdx.|Early Permian|Early Permian|Of Champion and Henin (1994). Previously mapped as part of Kalunga Granodiorite. Age: 282+/-15Ma, 276Ma and 280Ma (Rb-Sr). Mainly grey, fine- to medium-grained, slightly porphyritic, hornblende-biotite granodiorite; mafic enclaves to ~10cm common. I-type.||||||07-FEB-11
36171|Silver Pot Granodiorite|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|276 Ma (Rb/Sr isochron age).||||I-type granitoids.|
27567|Silver Valley Conglomerate|22497|6|Mentioned|p105|||||||||
27567|Silver Valley Conglomerate|23423|4|Described|Table 7.2 p300|Early Permian|Late Carboniferous|Also see p234. Overlain by Glen Gordon Volcanics. Underlain by Hodgkinson Formation - unconformable.||||||11-APR-07
27567|Silver Valley Conglomerate|23430|4|Described|p517|||Also see p504 Table 14.5. Overlain by Glen Gordon Volcanics.||||||11-APR-07
27567|Silver Valley Conglomerate|23431|6|Mentioned|p539|||Hodgkinson Province.||||||
27567|Silver Valley Conglomerate|23498|6|Mentioned|p21 table 1|||||||||
27567|Silver Valley Conglomerate|23506|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
27567|Silver Valley Conglomerate|23616|4|Described|Table 1C p12 p38||Carboniferous|Unconformably overlies Hodgkinson Formation; faulted against or apparently conformably overlain by Glen Gordon Volcanics. Underlain by Hodgkinson Formation - unconformable.||||||11-APR-07
27567|Silver Valley Conglomerate|30505|4|Described|p4|||See also p5 - 7,16. Carboniferous.||||||11-APR-07
27567|Silver Valley Conglomerate|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27567|Silver Valley Conglomerate|31832|6|Mentioned|Table 6|||||||||
27567|Silver Valley Conglomerate|32836|5|Briefly described|p8|||Age discussed||||||
27567|Silver Valley Conglomerate|33205|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27567|Silver Valley Conglomerate|37565|6|Mentioned|Fig.6|||||||||
27567|Silver Valley Conglomerate|37575|4|Described|p179|||See also Fig.2||||||
27567|Silver Valley Conglomerate|37613|6|Mentioned|Fig.1|||||||||
27567|Silver Valley Conglomerate|39445|5|Briefly described|Table 7|||||||||
27567|Silver Valley Conglomerate|40892|4|Described|p75|||||||||
27567|Silver Valley Conglomerate|42547|3|Fully described|p73|||||||||
27567|Silver Valley Conglomerate|43060|4|Described|p56,Table 1c||Carboniferous|||||||
27567|Silver Valley Conglomerate|43896|14|Not recorded|Map Legend||Carboniferous|||||||
27567|Silver Valley Conglomerate|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27567|Silver Valley Conglomerate|44296|14|Not recorded|Map Legend||Carboniferous|||||||
27567|Silver Valley Conglomerate|45065|4|Described|Table 4|||||||||
27567|Silver Valley Conglomerate|46845|6|Mentioned|Table 1|||||||||
27567|Silver Valley Conglomerate|60425|4|Described|p14 Tb. 1, p37|Early Permian|Late Carboniferous|Unconformably overlies Hodgkinson Fm; overlain by Glen Gordon Volcanics, probably conformably. Max. thickness: ~90m. Coarse polymictic conglomerate with subordinate volcanic sandstone + mudstone, containing glass shards; lenses of rhyolitic ignimbrite.||||||07-FEB-11
27567|Silver Valley Conglomerate|62371|5|Briefly described|p472 Fig.3|Carboniferous|Carboniferous|Mixed shallow marine sediments.||||||
27567|Silver Valley Conglomerate|63140|6|Mentioned|p572 fig 3|Carboniferous|Carboniferous|Hodgkinson Province.||||||
27567|Silver Valley Conglomerate|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province.||||||
27567|Silver Valley Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Balfes Creek, Ellenvale and Wade beds; Insolvency Gully and Marshs Creek Formations, are all mapped under the symbol, CPs.||||||
27567|Silver Valley Conglomerate|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.||||||
27567|Silver Valley Conglomerate|69592|5|Briefly described|p230, p242-243, p249, p297-298|Pennsylvanian|Pennsylvanian|Best (1962). Exposed in a small, fault-bounded graben west of Herberton in the southern Hodgkinson Province. Post-Tabberabberan Orogeny; beds dip gently. 100m thick. Sediment was sourced from local basement rocks of Hodgkinson Formation, with significant input from adjacent, coeval volcanism. The upper parts contain Pennsylvanian plant fossils (eg Botrychiopsis).||||Unconformably overlies Hodgkinson Formation.|Coarse, polymict, clast-supported conglomerate; subordinate medium- to coarse-grained volcaniclastic sandstone and mudstone contain numerous glass shards. Minor rhyolitic ignimbrite, air-fall tuff, and carbonaceous sandstone and siltstone lenses.|
27567|Silver Valley Conglomerate|70033|6|Mentioned|p52 Fig 8.1|Permian|Carboniferous|||||||
36690|Silverpot Granodiorite|23616|5|Briefly described|p68|||Rb-Sr biotite 276 Ma and 280 Ma.  Of Almaden Supersuite||||||
36690|Silverpot Granodiorite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|~280 Ma.|Almaden Supersuite.|||I-type.|
41617|Skeleton Creek Granite|60360|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Muscovite-biotite granite.||||||
41617|Skeleton Creek Granite|68477|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pama Province granitoids.|||||Locally foliated, pale grey muscovite-biotite granite.|
41617|Skeleton Creek Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
70018|Slaty Range Granite|61527|6|Mentioned|p791|||Granite of the Slaty Range pluton.||||||
36547|Sleeper Log Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 211.  I-Type.||||||
40138|Sleipner Member|24615|5|Briefly described|CD|Permian|Permian|[Pkcs].  Massive, poorly sorted, matrix to clast-supported, monomictic and lesser polymictic, granule to boulder breccia and minor conglomerate; volcanolithic sandstone, minor coal.||||||
40138|Sleipner Member|50209|5|Briefly described|Map Legend|Permian|Permian|Of the Berserker Group.||||||17-MAY-04
40138|Sleipner Member|50212|5|Briefly described|Map Legend|Permian|Permian|Of Chalmers Formation (Berserker Group)||||||
40138|Sleipner Member|61778|3|Fully described|p233, p234 Fig. 1, p236, p240 Fig. 11||Early Permian|Of Berserker Group. Consists of volcanic breccias and conglomerates. Geological Province: Berserker Subprovince. See p236 for detailed lithology.||||||07-FEB-11
40138|Sleipner Member|64429|2|Defined|p15, p21-22|Early Permian|Early Permian|Upper section of Chalmers Formation (Berserker Group). Previously defined as Sleipner Andesite Tuff (Taube 1979). Thickness: 360m. Intruded by Ellrott Rhyolite in places. Detailed lithology presented for this breccia-conglomerate unit. ||||||
40138|Sleipner Member|68008|2|Defined|p158-159, p167-170, p173|Permian|Permian|Originally the Sleipner Andesite Tuff of Taube (1979); named after a railway siding at Sleipner, ~15km E of Rockhampton. Part of the Berserker Series (Whitehouse, 1930), renamed the Berserker beds (Kirkegaard et al., 1970), which was divided into the Berserker Group (Crouch and Parfrey, 1998) including this unit. The type area is on the S side of Mount MacDonald; 360m thick. Marine mass flow deposits, proximal to Ellrott Rhyolite centres (source of this unit).||Chalmers Formation.||Is intruded by Ellrott Rhyolite.|Mainly dark green-grey, massive, poorly sorted, monomictic and lesser polymictic, granule to boulder breccia and minor conglomerate; interbedded with feldspatholithic sandstone and minor siltstone. Local andesitic lavas.|
40138|Sleipner Member|68679|5|Briefly described|p350|||Previously the Sleipner Andesite Tuff (Taube, 1979) and the Sleipner andesitic breccia (Hunns, 1994). Berserker Subprovince, Yarrol Province.||Chalmers Formation.|||Breccia and lesser sandstone and siltstone; andesitic fragments up to 2cm across, and locally rhyolite up to 30cm across.|
26142|Sly Creek Sandstone|22538|6|Mentioned|P714||Statherian|||||||
26142|Sly Creek Sandstone|22670|6|Mentioned|52|||Geological Province: McArthur Basin.||||||14-APR-08
26142|Sly Creek Sandstone|22853|3|Fully described|6|Proterozoic|Proterozoic|Geological Province: McArthur Basin. Of the Tawallah Group. Max thickness: 770 m. Underlain by Seigal Volcanics.||||||14-APR-08
26142|Sly Creek Sandstone|23065|5|Briefly described|16|||Geological Province: McArthur Basin. Of the Tawallah Group. Overlain by Aquarium Formation; underlain by McDermott Formation.||||||14-APR-08
26142|Sly Creek Sandstone|23197|6|Mentioned|p850|||Referred to as Yiyinti-Sly Creek Sandstone.||||||
26142|Sly Creek Sandstone|23363|5|Briefly described|344 Fig.3|||||||||
26142|Sly Creek Sandstone|23374|6|Mentioned|p42||Statherian|Equivalent to Gumarrirnbang Sandstone. Of the Tawallah Group; in the McArthur Basin.||||||04-DEC-06
26142|Sly Creek Sandstone|23395|5|Briefly described|p388 Fig.4|||||||||
26142|Sly Creek Sandstone|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
26142|Sly Creek Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26142|Sly Creek Sandstone|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with upper part of Kombolgie Subgroup (Katherine River Group).  Geological Province: McArthur Basin.||||||
26142|Sly Creek Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
26142|Sly Creek Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group.||||||14-APR-08
26142|Sly Creek Sandstone|24050|5|Briefly described|p16|||Of the Tawallah Group.  Geological Province: McArthur Basin.||||||04-DEC-06
26142|Sly Creek Sandstone|31421|6|Mentioned|p507|||||||||
26142|Sly Creek Sandstone|32660|5|Briefly described|Table 4|||||||||
26142|Sly Creek Sandstone|33665|6|Mentioned|p366|||See also p368.||||||04-DEC-06
26142|Sly Creek Sandstone|35114|6|Mentioned|p203|||||||||
26142|Sly Creek Sandstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|36012|3|Fully described|Table 2|||||||||
26142|Sly Creek Sandstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|37568|5|Briefly described|p78|||||||||
26142|Sly Creek Sandstone|38582|6|Mentioned|Fig.3|||||||||
26142|Sly Creek Sandstone|38584|4|Described|p14|||||||||
26142|Sly Creek Sandstone|39445|5|Briefly described|Table 2|||See also p36.||||||04-DEC-06
26142|Sly Creek Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26142|Sly Creek Sandstone|40489|6|Mentioned|p89|||||||||
26142|Sly Creek Sandstone|40691|5|Briefly described|p9|||||||||
26142|Sly Creek Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26142|Sly Creek Sandstone|41721|3|Fully described|p20|||Of the Tawallah Group. Thickness: 320m. Conformably overlies McDermott Formation, grading into glaucontic sandstone of the Aquarium Formation above. Geological province: McArthur Basin. Sandstone, fine- to medium-grained, laminated, well sorted...........||||||01-AUG-07
26142|Sly Creek Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26142|Sly Creek Sandstone|42385|3|Fully described|p6-7, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Tawallah Group. Includes Rosie Creek Sandstone Mbr. Conformable over Seigal Volcanics. Max. thick: 770m. Sandstone, very fine- to very coarse-grained, conglomeratic sandstone feldspathic in places; arkosic ferruginous or galuconitic.||||||18-SEP-07
26142|Sly Creek Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
26142|Sly Creek Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.|Includes: Rosie Creek Sandstone Member at top.|In schematic section, underlies Aquarium Formation; overlies Seigal Volcanics.|Quartzarenite, pebble beds common in upper part; minor siltstone and shale. Detailed lithology given.|09-NOV-11
26142|Sly Creek Sandstone|42639|3|Fully described|p10 Table 4 p11|||||||||
26142|Sly Creek Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
26142|Sly Creek Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Quartzarenite, white to pale pink, mainly fine to medium grained and thin to very thick bedded with rare quartz pebble beds.||||||19-OCT-05
26142|Sly Creek Sandstone|42812|3|Fully described|p11, Table 3|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterzoic" age.||||||04-DEC-06
26142|Sly Creek Sandstone|43036|3|Fully described|p15|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|44287|14|Not recorded|p.8, opp.7|||(E53-3).||||||
26142|Sly Creek Sandstone|44288|14|Not recorded|map legend||Paleoproterozoic|Quartz sandstone, pebbly bands, minor siltstone. Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44305|14|Not recorded|p.6,12|||(E53-8). opp.p.6,18.||||||
26142|Sly Creek Sandstone|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44473|14|Not recorded|p.8, opp. p.7|||(E53-7).||||||
26142|Sly Creek Sandstone|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44530|14|Not recorded|p.4,8, opp.8|||(D53-15).||||||
26142|Sly Creek Sandstone|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|45162|2|Defined|p19|Proterozoic|Proterozoic|Revised herein. Rosie Creek Sandstone incorporated into Sly Creek Sandstone.||||||21-FEB-18
26142|Sly Creek Sandstone|45166|5|Briefly described|p28|||||||||
26142|Sly Creek Sandstone|46804|6|Mentioned|p154|||||||||
26142|Sly Creek Sandstone|49001|6|Mentioned|p5|||||||||
26142|Sly Creek Sandstone|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
26142|Sly Creek Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Includes Rosie Creek Sandstone Member. Overlain by Aquarium Formation, underlain by Seigal Volcanics.||||||
26142|Sly Creek Sandstone|62082|5|Briefly described|p115|Proterozoic|Proterozoic|Geological Province: Carpentaria Terrain.||||||07-FEB-11
26142|Sly Creek Sandstone|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin. Shown as Sly Ck Sst.||||||
26142|Sly Creek Sandstone|63112|5|Briefly described|p1190-1192, Tb.1, p1194, p1206|||Leichhardt Superbasin. Age approximated from Fig.2. 200-770 m thick.|c.1755-1760 Ma.||||Pebblestone conglomerates and coarse-grained pebbly sandstones overlain by a semi- to supermature quartzarenite, which is in turn overlain by coarser grained pebbly sandstones.|
26142|Sly Creek Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
26142|Sly Creek Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p370 |||A SW-thickening siliciclastic apron west of a basaltic volcanic zone in the Murphy Tectonic Ridge.||Of the Tawallah Group.|Includes Rosie Creek Sandstone Member.|||
26142|Sly Creek Sandstone|65228|5|Briefly described|p21, Figs.02, 05, 06, 07.|||McArthur Basin.||Unit in Tawallah Group.||Equivalent to McDermott Formation.||
26142|Sly Creek Sandstone|65337|6|Mentioned|p14. |||Southern McArthur Basin. Correlated with Gator Sandstone. Contains a local basalt interval.||||||
26142|Sly Creek Sandstone|65340|4|Described|p12 Fig.6. |||Revised in this study. Defined by Roberts et al. (1963) and Ahmad and Wygralak (1989); this study removes the unit underlying the Aquarium Formation throughout the Wearyan Shelf, and incorporates it into the Wununmantyala Sandstone [??].||Unit in Tawallah Group.|Includes Rosie Creek Sandstone Member.|Overlies Seigal Volcanics. Is overlain by McDermott Formation.||21-FEB-18
26142|Sly Creek Sandstone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming.||Unit in Tawallah Group.||Overlies McDermott Formation. Is overlain by Settlement Creek Volcanics.|Fine- to medium-grained quartz arenite; pebble beds common in upper part; planar to trough cross-beds, channel-lag deposits, ripples, minor graded bedding, rare dessication cracks; minor thinly-bedded siltstone and shale, commonly micaceous.|
26142|Sly Creek Sandstone|67323|4|Described|GIS attrib tbl, Solid Geology Map, p31|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin.|1787 +/- 17 Ma (maximum depositional age).|Tawallah Group.||Overlies Seigal Volcanics.|White, pink or grey massive medium-grained quartzose sandstone, pebbly sandstone, conglomerate.|
26142|Sly Creek Sandstone|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. 900 m thick. Forms prominent ridges.||Tawallah Group||Cconformably overlies McDermott Formation or Seigal Volcanics. Overlain conformably by Settlement Creek Volcanics.|Very fine- to very coarse-(mainly medium)-grained quartz arenite: glauconitic, feldspathic, arkosic; minor pebbly sandstone, conglomerate, micaceous siltstone, shale, chert breccia, dolarenite.|
26142|Sly Creek Sandstone|67564|5|Briefly described|p86.|||Southern McArthur Basin.||Unit in Tawallah Group.|Includes Rosie Creek Member.|||
26142|Sly Creek Sandstone|67779|5|Briefly described|p36.|||Lower parts are correlated with Gumarrirnbang Sandstone.|1787 +/- 17 Ma (Hollis et al. 2010a).|Unit in Tawallah Group.||||
26142|Sly Creek Sandstone|69383|5|Briefly described|p52-54||Paleoproterozoic|McArthur Basin. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1787+/-17 Ma||||An orange, medium-grained sandstone with prominent wave ripple-marks was sampled from top of unit.|
26142|Sly Creek Sandstone|69430|4|Described|p15:3, 10-12|||The previous definition was replaced by Wununmantyala Sandstone (as defined by Pietsch et al., 1991); the name is now used for the succession overlying the Seigal Volcanics in the Batten Fault Zone and SW McArthur Basin. 320m thick (also said to be up to 900m thick with Rosie Creek Sandstone Member). Nearshore shallow-marine deposits. Is stated to conformably overlie McDermott Formation, but this contradicts the relationships shown in Fig.15.4, and is inconsistent with Sly Creek Sandstone being correlated with upper Seigal Volcanics which conformably underlies McDermott Formation.||Tawallah Group.|Rosie Creek Sandstone Member.|Overlies Seigal Volcanics. Is overlain conformably and gradationally by Aquarium Formation. Correlated with upper Seigal Volcanics.|White, pink or grey massive medium-grained quartz sandstone, pebbly sandstone, conglomerate.|12-JUL-16
26142|Sly Creek Sandstone|69591|5|Briefly described|p39, p58|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession. Alluvial braidplain deposits.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|White, pink or grey massive medium-grained quartzose sandstone, pebbly sandstone, conglomerate.|
26142|Sly Creek Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group|Includes Rosie Creek Sandstone Member|Overlies Seigal Volcanics||
26142|Sly Creek Sandstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies McDermott Formation. Is overlain by Aquarium Formation.|Lithic and quartz sandstone, fine- to medium-grained, flaggy, locally feldspathic; minor conglomerate.|
26142|Sly Creek Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1787+/-17 Ma (MDA: U-Pb zircon LA-ICPMS).||||Ripple-martked sandstone.|
26142|Sly Creek Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group||Partially overlies and is laterally equivalent to Seigal Volcanics and underlies Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by and partly equivalent to Seigal Volcanics. Overlain by Rosie Creek Sandstone Member. Equivalent[?] to Carolina Sandstone Member.||
26142|Sly Creek Sandstone|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Shown as Sly Creek Formation p19.||Tawallah Group||Partially overlies Seigal Volcanics and underlies Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.||Tawallah Group||Underlain by and partly correlated to Seigal Volcanics. Overlain by Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|73412|5|Briefly described|p4, 8-9, 14|||Southern McArthur Basin. Non-magnetic.||Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Rosie Creek Sandstone.||
72735|Smallcombes Road Granite|65452|6|Mentioned|p6 Fig.2, p22|Late Triassic|Late Triassic|Part of Agnes Water Caldera Complex. High-level emplacement.||||||
72735|Smallcombes Road Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink, moderately porphyritic, fine-grained biotite granite.|
72735|Smallcombes Road Granite|68679|5|Briefly described|p432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Pink, moderately porphyritic, fine-grained biotite granite.|
30355|Smedley Dacite|22675|4|Described|p73|Early Permian|Early Permian|~297Ma,  Bulgonunna Volcanic Group||||||
30355|Smedley Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V75. I-Type.||||||
30355|Smedley Dacite|43259|5|Briefly described|Appendix 1,p7||Late Carboniferous|||||||
30355|Smedley Dacite|43391|5|Briefly described|Map legend||Late Carboniferous|Of the Bulgonunna Volcanic Group.  Dacitic ignimbrite.  Geological Province: Coastal Ranges Igneous Province.||||||23-JUN-04
30355|Smedley Dacite|43727|5|Briefly described|Table 14,p50|||||||||
30355|Smedley Dacite|43734|6|Mentioned|p6|||U-Pb age: 297.3+/-4.8 Ma||||||
30355|Smedley Dacite|60659|5|Briefly described|p16|Early Permian|Early Permian|Of the Bulgonunna Group. Moderately crystal-rich, lithic clast-poor to lithic-rich wedled dacoitic ignimbrite. Age: ~297Ma. Part of the Smedley association. Of the Bulgonunna Province.||||||07-FEB-11
30355|Smedley Dacite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
30355|Smedley Dacite|70740|4|Described|i, iv, p8, p82 fig 50, p84|Early Permian|Late Carboniferous|Drummond Basin. SHRIMP age derived from Black (1994). Includes areas formerly mapped as Smedley Association subunits. Distribution is discussed, petrography described in detail. A type area at Burdekin Falls Dam is mentioned and briefly described. See also p86, p87, p92, p105-p109, p111, p125.|297.3 +/- 4.8 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Intruded by the Glendon Granodiorite. Overlain by the Arundel Rhyolite.|Crystal to locally lithic-rich, strongly welded dacitic ignimbrite. Characterised by abundant, complexly-zoned plagioclase and euhedral crystal-rich blebs.|
75150|Smith granite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name. Of the Bedarra Suite (Bedarra Batholith or Supersuite?) in the Bedarra Granite Belt. Pale grey to pale brown (iron stained), medium-grained, slightly to moderately porphyritic biotite granite. I-type.||||||07-FEB-11
75733|Smoko Creek Granite|70740|5|Briefly described|p112, p129|||Distribution and outcrop characteristics briefly discussed on p129. |||||Medium-grained, porphyritic biotite monzogranite with traces of hornblende, sphene and allanite.|
68737|Smoky Creek beds|60282|5|Briefly described|p10|||On the SCORIA and BANANA map sheets. May be equivalent of Rookwood Volcanics?||||||
40139|Smoky beds|24615|5|Briefly described|CD|Early Permian|Early Permian|[Ps].  Andesitic conglomerate and sandstone, mudstone, minor andesitic lava.||||||
40139|Smoky beds|50197|5|Briefly described|Map Legend|Permian|Permian|||||||
40139|Smoky beds|50215|5|Briefly described|Map Legend|Early Permian|Early Permian|Andesitic conglomerate and sandstone, mudstone and minor andesite lava.||||||18-JUN-09
40139|Smoky beds|65388|6|Mentioned|p35|Early Permian||Yarrol Province. Correlated with Yaparaba Volcanics.||||||
40139|Smoky beds|68008|2|Defined|p130, p132, p134-135, p144-147, p183-184|Permian|Permian|See also p366, p368-369, p626. Named after Smoky Creek. The type section is along Smoky Creek, from GR2451000E 7331500N to GR255900E 7333100N. Includes rocks mapped as Owl Gully Volcanics by Dear et al. (1971) and forms the majority of their Mount Gerard Complex. Forms hilly topography with some benches and flat-topped hills. At least 150m thick. Unfossiliferous. Suggested Artinskian age from its position above Youlambie Conglomerate. Probable correlative of Owl Gully Volcanics. Hosts a number of small gold deposits. Geophysics modelling.||||Conformably overlies Yarrol Formation or Youlambie Conglomerate. Underlies and/or faulted against Inverness Volcanics. Is intruded by, and partly overlies, the Craiglands Quartz Monzodiorite.|mainly volcaniclastic conglomerate and breccia with andesitic to dacitic clasts; typically matrix supported; minor feldspathic sandstone, siltstone and shale. Local andesite intrusions, flows and tuffs near Bell Creek.|
40139|Smoky beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince. This unit, with the Narayen and Nogo beds, and the Yaparaba Volcanics, are all mapped under the symbol, Pvy.||||||
40139|Smoky beds|68679|5|Briefly described|p312-313, p338, p343-344, p352, p425|Permian|Permian|Murray et al. (2012). Includes some rocks mapped as Owl Gully Volcanics by Dear et al. (1971). Forms a thin roof pendant that partly covers, and is intruded by, the Craiglands Quartz Monzodiorite. Northern New England Orogen.||||Overlies and is intruded by Craiglands Quartz Monzodiorite.|Mainly volcaniclastic conglomerate (clasts to 1m) and breccia with andesitic to dacitic clasts, typically matrix-supported; very minor medium- and fine-grained feldspathic sandstone, siltstone and shale; andesite flows and intrusions mainly in the S.|
36224|Soda Spring Granite|23291|5|Briefly described|p101 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Froghollow Suite. Intrudes Brookers Waterhole Granite. Geological Province: Georgetown Region.||||||08-JUL-15
36224|Soda Spring Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36224|Soda Spring Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 372. I-Type.||||||
36224|Soda Spring Granite|23624|4|Described|p14|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||17-DEC-13
36224|Soda Spring Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey to pale pink, medium-grained, porphyritic biotite monzogranite; with scattered K-feldspar megacrysts and mafic enclaves.|
36224|Soda Spring Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey to pale pink, medium-grained, porphyritic biotite monzogranite; with scattered K-feldspar megacrysts and mafic enclaves.|
22862|Solanum Granodiorite|23423|6|Mentioned|p306 Table 7.3|||||||||
22862|Solanum Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of the Almaden Supersuite.||||||01-JUN-09
22862|Solanum Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 276. I-Type.||||||
22862|Solanum Granodiorite|23616|6|Mentioned|Table 3 p48|||See also p99 Appendix 2.||||||
22862|Solanum Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). medium to dark grey, medium to fine, abundantly porphyritic biotite-hornblende granodiorite.||||||15-JUN-06
22862|Solanum Granodiorite|43259|4|Described|Appendix 1,p35.||Late Carboniferous|||||||
22862|Solanum Granodiorite|60425|4|Described|p49 Tb.3, p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Intruded Boonmoo Volcanic Subgroup. Medium to dark grey,medium- to fine-grained, highly porphyritic biotite-hornblende granodiorite. I-type.||||||07-FEB-11
26144|Soldiers Cap Group|22455|6|Mentioned|p 15|||||||||
26144|Soldiers Cap Group|22460|4|Described|p446, 448|||Inferred from a U-Pb zircon age of 1677+/-9 Ma for the conformably underlying Fullerton River Group (Page, 1988).||||||
26144|Soldiers Cap Group|22461|5|Briefly described|Fig 1 p464|||||||||
26144|Soldiers Cap Group|22465|5|Briefly described|p934|||||||||
26144|Soldiers Cap Group|22467|4|Described|Fig 2 p431, 432, 443|||||||||
26144|Soldiers Cap Group|22468|5|Briefly described|p 16, 17|||||||||
26144|Soldiers Cap Group|22483|6|Mentioned|p418.|||||||||
26144|Soldiers Cap Group|22513|4|Described|p.373-385|Statherian||Age: ca 1677 Ma.||||||06-FEB-07
26144|Soldiers Cap Group|22514|6|Mentioned|p394|||||||||
26144|Soldiers Cap Group|22515|6|Mentioned|p402,407|||||||||
26144|Soldiers Cap Group|22523|4|Described|p363,365-366||Calymmian|Max Age: 1584 Ma.||||||06-FEB-07
26144|Soldiers Cap Group|22533|6|Mentioned|p53|||||||||
26144|Soldiers Cap Group|22568|6|Mentioned|p327|||||||||
26144|Soldiers Cap Group|22667|6|Mentioned|P237|||||||||
26144|Soldiers Cap Group|22692|5|Briefly described|p765, Fig.2 p766|||Age of unit 1677+/-9 Ma (Page, 1993)||||||
26144|Soldiers Cap Group|22735|5|Briefly described|p281||Statherian|Metasiliciclastic unit of Mt Isa Group part of the Moronan Supergroup.||||||06-FEB-07
26144|Soldiers Cap Group|22739|6|Mentioned|169|Proterozoic|Proterozoic|Geol Province Mount Isa Inlier||||||
26144|Soldiers Cap Group|22961|5|Briefly described|p80||Paleoproterozoic|||||||07-NOV-08
26144|Soldiers Cap Group|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the upper sequence of the Willyama Supergroup, and upper sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
26144|Soldiers Cap Group|23064|6|Mentioned|136|||||||||
26144|Soldiers Cap Group|23067|5|Briefly described|p793 (fig 1)|||||||||
26144|Soldiers Cap Group|23068|5|Briefly described|p783||Mesoproterozoic|||||||
26144|Soldiers Cap Group|23069|5|Briefly described|p775 (fig 1)|||||||||
26144|Soldiers Cap Group|23333|5|Briefly described|1115 Fig.2|Statherian|Statherian|||||||
26144|Soldiers Cap Group|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|||||||
26144|Soldiers Cap Group|23425|6|Mentioned|p380, Table 9.7 p395.|||||||||
26144|Soldiers Cap Group|23458|6|Mentioned|p115|||Undivided portion intruded by Dipvale Granodiorite.||||||27-AUG-07
26144|Soldiers Cap Group|23471|5|Briefly described|p111|||Of Maronan Supergroup. Geological Province: Mount Isa Block.||||||
26144|Soldiers Cap Group|23519|5|Briefly described|p106 Fig 1|Mesoproterozoic|Mesoproterozoic|See also page 110 Table 1. Geological Province: Eastern Fold Belt.||||||
26144|Soldiers Cap Group|23613|6|Mentioned|p724 Fig. 1|||Parent: Maronan Supergroup||||||
26144|Soldiers Cap Group|23901|6|Mentioned|p1685|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
26144|Soldiers Cap Group|23962|5|Briefly described|p1213, 1215 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Of the Maronan Supergroup.||||||16-DEC-04
26144|Soldiers Cap Group|23966|4|Described|p1308|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Maronan Supergroup. Overlies: Fullarton River Group.  Age: 1677 +/- 9Ma.||||||25-JUN-09
26144|Soldiers Cap Group|23967|6|Mentioned|p1331|||Intruded by Saxby Granite.||||||
26144|Soldiers Cap Group|23970|5|Briefly described|p1391|||Geological Province: Mount Isa Inlier. Of the Maronan Supergroup.||||||02-MAR-05
26144|Soldiers Cap Group|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Maronan Supergroup||||||
26144|Soldiers Cap Group|23973|5|Briefly described|p1436 Fig. 1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Formerly known as the Kuridala Formation.||||||20-MAR-18
26144|Soldiers Cap Group|23974|5|Briefly described|p1450|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||16-DEC-04
26144|Soldiers Cap Group|23975|5|Briefly described|p1464|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Maronan Supergroup||||||
26144|Soldiers Cap Group|24032|6|Mentioned|p5, p6 Tb. 1, p12, p18|Proterozoic|Proterozoic|Includes meta-sediments and meta-volcanics.||||||
26144|Soldiers Cap Group|24156|5|Briefly described|p30||||||||Foliated quartz-garnet gneiss.|
26144|Soldiers Cap Group|24168|6|Mentioned|p640|Proterozoic|Proterozoic|||||||
26144|Soldiers Cap Group|24197|5|Briefly described|p132|||Contains Fe-tholeiite. Age: ~1700-1650Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
26144|Soldiers Cap Group|24253|5|Briefly described|p4, p10 Fig.4|Proterozoic|Proterozoic|Age: ~1670Ma. Geological Province: Mount Isa Block.||||||
26144|Soldiers Cap Group|24254|5|Briefly described|p19 Fig.2|||Geological Province: Mount Isa Block.||||||
26144|Soldiers Cap Group|24256|5|Briefly described|p47|Statherian|Statherian|Age: 1676 +/- 5Ma. Geological Province: Mount Isa Block||||||
26144|Soldiers Cap Group|24257|6|Mentioned|p68|||Geological Province: Eastern fold belt, Mount Isa Block. Formation is Fm. in text.||||||
26144|Soldiers Cap Group|24258|5|Briefly described|p93|Statherian|Statherian|Age: ca. 1670 Ma. Geological Province: Mount Isa Inlier||||||
26144|Soldiers Cap Group|24259|5|Briefly described|p106|Proterozoic|Proterozoic|Geological Province: Mount Isa Block. Age: ~1670Ma||||||
26144|Soldiers Cap Group|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Geological Province: Eastern Fold Belt.||||||
26144|Soldiers Cap Group|24462|5|Briefly described|p295|||Of the Maronan Supergroup.  Geological Province: Mount Isa Block.||||||
26144|Soldiers Cap Group|30530|6|Mentioned|p516|||||||||
26144|Soldiers Cap Group|30531|6|Mentioned|p15|||Also mention p17 and p22.||||||20-MAR-18
26144|Soldiers Cap Group|30532|6|Mentioned|p113|||||||||
26144|Soldiers Cap Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26144|Soldiers Cap Group|32660|4|Described|Table 5|||||||||
26144|Soldiers Cap Group|32959|6|Mentioned|Fig.21|||||||||
26144|Soldiers Cap Group|33900|5|Briefly described|p16|||See also p4.||||||06-FEB-07
26144|Soldiers Cap Group|35074|6|Mentioned|Fig.2|||||||||
26144|Soldiers Cap Group|35295|2|Defined|p602|Precambrian|Precambrian|||||||
26144|Soldiers Cap Group|35388|6|Mentioned|p89|||Also see Fig.10||||||
26144|Soldiers Cap Group|35536|6|Mentioned|p26|||||||||
26144|Soldiers Cap Group|35950|6|Mentioned|p305|||||||||
26144|Soldiers Cap Group|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
26144|Soldiers Cap Group|37462|4|Described|Table4.VII|||||||||
26144|Soldiers Cap Group|37565|5|Briefly described|p2|||See also Fig.5||||||
26144|Soldiers Cap Group|37568|4|Described|p81|||See also p85.||||||06-FEB-07
26144|Soldiers Cap Group|37569|6|Mentioned|p90|||||||||
26144|Soldiers Cap Group|37645|5|Briefly described|p5.12.3|||See also Fig.3||||||
26144|Soldiers Cap Group|37696|6|Mentioned|p427|||||||||
26144|Soldiers Cap Group|37862|6|Mentioned|p587|||||||||
26144|Soldiers Cap Group|38234|4|Described|p104|||||||||
26144|Soldiers Cap Group|38275|6|Mentioned|p181|||||||||
26144|Soldiers Cap Group|38276|6|Mentioned|p168|||See also Fig.1.||||||
26144|Soldiers Cap Group|38278|6|Mentioned|Fig.1|||||||||
26144|Soldiers Cap Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26144|Soldiers Cap Group|38834|6|Mentioned|p162|||||||||
26144|Soldiers Cap Group|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||06-FEB-07
26144|Soldiers Cap Group|39127|6|Mentioned|p169|||||||||
26144|Soldiers Cap Group|39202|6|Mentioned|Fig.2|||||||||
26144|Soldiers Cap Group|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26144|Soldiers Cap Group|39445|6|Mentioned|p41|||Correlation. See also Table 2||||||
26144|Soldiers Cap Group|39496|5|Briefly described|p7|||||||||
26144|Soldiers Cap Group|39566|6|Mentioned|p57|||||||||
26144|Soldiers Cap Group|39622|6|Mentioned|p19|||||||||
26144|Soldiers Cap Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
26144|Soldiers Cap Group|39924|6|Mentioned|p348|||||||||
26144|Soldiers Cap Group|40623|5|Briefly described|p95|||See also p111.||||||06-FEB-07
26144|Soldiers Cap Group|40648|3|Fully described|p8|||Previously mapped as Corella Formation||||||
26144|Soldiers Cap Group|40840|6|Mentioned|Map legend|||||||||
26144|Soldiers Cap Group|41081|6|Mentioned|p104|||||||||
26144|Soldiers Cap Group|41272|5|Briefly described|M 1of1 M06|||Mention M 1of1 C07||||||
26144|Soldiers Cap Group|41306|3|Fully described|p6|||||||||
26144|Soldiers Cap Group|41464|6|Mentioned|Map legend|Proterozoic||||||||
26144|Soldiers Cap Group|41556|6|Mentioned|Map legend|Proterozoic||||||||
26144|Soldiers Cap Group|41568|4|Described|p5|||||||||
26144|Soldiers Cap Group|41978|3|Fully described|Table 1 p492|||||||||20-MAR-18
26144|Soldiers Cap Group|41979|6|Mentioned|p527|||||||||
26144|Soldiers Cap Group|42556|5|Briefly described|p1|||Of Maronan Supergroup.||||||06-FEB-07
26144|Soldiers Cap Group|42565|5|Briefly described|p2, Fig.4 p4, p3|||||||||
26144|Soldiers Cap Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Greywacke, siltstone, sandstone, mafic volcanics.||||||09-FEB-09
26144|Soldiers Cap Group|42755|5|Briefly described|p5|||||||||
26144|Soldiers Cap Group|42766|6|Mentioned|p1, p2|||||||||
26144|Soldiers Cap Group|42812|6|Mentioned|p65|||||||||
26144|Soldiers Cap Group|43490|6|Mentioned|9|||Metamorphic biotite age: 1568Ma||||||
26144|Soldiers Cap Group|43612|6|Mentioned|p35|||||||||
26144|Soldiers Cap Group|43614|6|Mentioned|p18|||||||||
26144|Soldiers Cap Group|43615|6|Mentioned|p15|||||||||
26144|Soldiers Cap Group|43616|6|Mentioned|p2|||||||||
26144|Soldiers Cap Group|43618|6|Mentioned|p41|||||||||
26144|Soldiers Cap Group|43620|6|Mentioned|Fig.1,p51|||||||||
26144|Soldiers Cap Group|43928|6|Mentioned|24|||||||||
26144|Soldiers Cap Group|44195|4|Described|Fig.1,p344,349|||p345, Table 1.||||||
26144|Soldiers Cap Group|45136|6|Mentioned|p64|||||||||
26144|Soldiers Cap Group|45161|4|Described|p41|||||||||
26144|Soldiers Cap Group|45166|4|Described|p24|||||||||
26144|Soldiers Cap Group|46801|6|Mentioned|p126|||See also Fig. 14||||||
26144|Soldiers Cap Group|46919|6|Mentioned|p213|||||||||
26144|Soldiers Cap Group|46962|4|Described|Table 1|||See also Fig.3.||||||
26144|Soldiers Cap Group|49009|6|Mentioned|p12|||||||||
26144|Soldiers Cap Group|49041|5|Briefly described|Table 3|||||||||
26144|Soldiers Cap Group|49897|5|Briefly described|o21|||Geological Province: Eastern Fold Belt.||||||
26144|Soldiers Cap Group|50100|5|Briefly described|p11, p13 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Maronan Supergroup.  Includes the Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics and Kuridala Formation.  Age: 1695-1600Ma.  See also p35, p46.||||||07-NOV-08
26144|Soldiers Cap Group|50125|5|Briefly described|p85, p88|Paleoproterozoic|Paleoproterozoic|Age: 1690-1670 Ma. Geological Province: Eastern Succession, Mount Isa Inlier||||||07-NOV-08
26144|Soldiers Cap Group|50332|5|Briefly described|p16, p61, p96|Paleoproterozoic|Paleoproterozoic|Includes: Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics, Roxmere Quartzite, Marimo Slate. Age: 1695-1600Ma. Geological Province: Eastern Fold Belt Province. Metamorphosed and deformed rocks.||||||07-FEB-11
26144|Soldiers Cap Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Toole Creek Volcanics, Mount Norna Quartzite, Llewellyn Creek Formation.||||||
26144|Soldiers Cap Group|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Eastern Fold Belt.||||||03-JUN-09
26144|Soldiers Cap Group|60658|5|Briefly described|p61, p62 Fig.1|Proterozoic|Proterozoic|||||||
26144|Soldiers Cap Group|60665|5|Briefly described|p1146, p1149 Tb.2, p1150, p1163, p1169. |Statherian|Statherian|Siliciclastic metasedimentary and mafic metavolcanic rocks. Hosts Osborne, Eloise and Mount Elliott Cu-Au deposits.|c.1670 to 1650 Ma||||Feldspathic to pelitic schist, amphibolite and ironstone. Psammite, pelite, amphibolite. Graphitic schist and amphibolite.|
26144|Soldiers Cap Group|61736|5|Briefly described|p667 Tb. 1|Paleoproterozoic|Paleoproterozoic|Age of host succession of Pinnacles mineral deposit: </-1670Ma. Geological province: Mount Isa Inlier (eastern succession).||||||24-FEB-10
26144|Soldiers Cap Group|61922|5|Briefly described|p8, p9 Fig. 3|||Include: Toole Creek Volcanics, Mount Norna Quartzite and Llewellyn Creek Formation.  Geological Province: Mount Isa Inlier/Eastern Fold Belt. See also p12 Fig. 5. ||||||
26144|Soldiers Cap Group|61924|5|Briefly described|p50|||Part of the Maronan Supergroup. Age range: ca 1712 to ca 1676 Ma; and 1654+/-4 Ma for a metarhyolite.||||||
26144|Soldiers Cap Group|61925|5|Briefly described|p57 Fig. 2|||Comprises Llewellyn Creek Formation and Mount Norna Quartzite. Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||22-JUL-13
26144|Soldiers Cap Group|61926|5|Briefly described|p70-71, p84|||Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier. ||||||
26144|Soldiers Cap Group|61927|5|Briefly described|p92 Fig.1, p93|||Geological Province: Mount Isa Inlier.||||||
26144|Soldiers Cap Group|61928|5|Briefly described|p115|Proterozoic|Proterozoic|Multiply deformed and metamorphosed metasedimentary rocks and mafic meta-igneous rocks; the Osborne Cu-Au deposit is hosted predominantly in feldspathic psammite and pelite.||||||28-APR-06
26144|Soldiers Cap Group|61929|5|Briefly described|p125, p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Part of the Maronan Supergroup. Includes Toole Creek Formation. Metasupracrustal rocks that host the Canning Ag-Pb-Zn deposit and several iron oxide deposits. Age: ca1712-1655Ma. Geological Province: Calvert Superbasin.||||||06-MAY-13
26144|Soldiers Cap Group|61933|5|Briefly described|p175|||||||||
26144|Soldiers Cap Group|61936|5|Briefly described|p195 Fig. 6|Paleoproterozoic|Paleoproterozoic|Includes Llewellyn Creek Formation, Mount Norna Quartzite and Toole Creek Volcanics.||||||21-APR-10
26144|Soldiers Cap Group|61963|6|Mentioned|p776|||Hosts the Cannington Ag-Pb-Zn deposits.||||||23-MAR-06
26144|Soldiers Cap Group|62047|5|Briefly described|p90 Fig.1, p91 Fig. 2||||c. 1712-1650|||||
26144|Soldiers Cap Group|62084|6|Mentioned|p954|||Small lead- and zinc-rich prospects.||||||
26144|Soldiers Cap Group|62535|5|Briefly described|p667, p673|||Mount Isa eastern succession. Hosts strata-bound-stratiform Broken Hill-type Pb-Zn-Ag deposits (Cannington, Pegmont, Fairmile?).|c.1658 - c.1653 Ma.|||||
26144|Soldiers Cap Group|63110|6|Mentioned|p1130|||Age: ca 1676Ma (Page and Sun, 1998). Contains amphibolite and metabasalt along with minor felsic units, within a sequence dominated by metapelite and metapsammite (Beardsmore et al., 1988).||||||22-JUL-13
26144|Soldiers Cap Group|63866|5|Briefly described|p61, p63-p64, p70|||Numeric ages are interpreted as depositional ages and suggest that this group is equivalent to the Myally Supersequence in the Leichhardt River Fault Trough. According to the authors this group is referred to as the Gandry Dam Gneiss in the Cannington area. Numeric ages derived from Page and Sun, 1998.|1775 +/- 4 ma and 1774 +/- 4 Ma ||Includes the Llewellyn Creek Formation, Mounta Norna Quartzite and Toole Creek Volcanics.|||
26144|Soldiers Cap Group|63884|5|Briefly described|p14|||Includes Toole Creek Formation. Siliciclastic metasedimentary and metabasaltic.||||||
26144|Soldiers Cap Group|64248|5|Briefly described|p32,p33 Fig.1, p36,p38 Fig.5, p40 Fig.6|||See also p41 Tb. 2, p43 Fig.11, p45. Thickens considerably to the east. Foster and Austin (2008) proposed including Kuridala Formation in this unit, and moving Llewellyn Creek Formation out and below.|||Kuridala Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Equivalent to Mount Albert Group (lateral facies variation).||11-DEC-17
26144|Soldiers Cap Group|64249|5|Briefly described|p83, p86, p91, p97, p102, p103|Paleoproterozoic|Paleoproterozoic|Age: deposition between 1677 and 1654Ma. Geological Province: Mount Isa Inlier. Believed to be lateral equivalent of Young Australia Group.||||||22-JUL-13
26144|Soldiers Cap Group|64250|4|Described|Figs.3-5,8,10; p7, p13-14, p19-20|||Cloncurry Fold Belt, Mount Isa Inlier. These authors include Blake's (1987) 3 units as well as Kuridala Formation; further, Fullarton River Group is correlative of Soldiers Cap Group.|c.1675-1650 Ma||Includes Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics, Kuridala Formation.||Includes voluminous mafic volcanics and related dykes and sills; only minor felsic volcanism.|
26144|Soldiers Cap Group|64251|4|Described|p51 Fig. 1, p52, p54-56, p58, p60-63|||In contact with Doherty Formation (faulted). Geological Province: Mount Isa Inlier. Consists mostly of quartzite, muscovite and biotite schist, gneiss and migmatites.||||||
26144|Soldiers Cap Group|64252|5|Briefly described|p70 Fig. 1, p71-74, p76-77|||Age: 1666+/-14 Ma (Giles and Nutman, 2002). Geological Province: Mount Isa Inlier.||||||
26144|Soldiers Cap Group|64744|5|Briefly described|pp353-356, p363.|Statherian|Statherian|Mount Isa Basin. Basaltic intrusions aged 1690-1670 Ma.|1685 Ma.||||Deep marine, commonly carbonaceous, turbidite sequences. Extensively intruded by basaltic dykes and sills.|
26144|Soldiers Cap Group|65387|5|Briefly described|p3 Tb.1, p81-82|Statherian|Statherian|A metarhyolite unit in Foxes Creek area was dated at c.1654 Ma, and a sample of Toole Creek Volcanics at c.1660 Ma (both Neumann, 2007). Included a package of undivided gneisses, schists and quartzites of the Boomarra Horst with a minimum age 1776 +/- 8 Ma. This precludes them from being correlates of the Soldiers Cap Group, as previously thought. Gandry Dam Gneiss is a higher-grade equivalent.|c.1680-1655 Ma (Page and Sun, 1998; Neumann, 2007)||Includes Toole Creek Volcanics.|||
26144|Soldiers Cap Group|65396|4|Described|p4, p7, p9-10, p12, p15-16, p21, p23,p25|Statherian|Statherian|See also p27-29, p35-36, p55, p79, p81-82, p84-85, p88, p90-91, p99, p104-105, p109, p118, p120, p155, p159-161, p169-170, p173-180, p182-184, p188, p190, p193, p196-199, p201-202, p213, p217, p221-224, p226, p234-241, p264-266, p271, p273-276, p278, p280-281, p283-285, p292-293, p299, p311-312, p318, p321, p327-330, p333, p335, p337, p343-345, p356, p364, p388-389, p391, p399, p439-440, p496. Mount Isa Inlier: Eastern Succession. The authors propose moving this Group from Cover Sequence 2 to younger (c.1675-1650 Ma) Cover Sequence 3, as well as removing Llewellyn Creek Formation. The Group is, however, given an age of 1686 Ma on p28. Also, older sequences in the Boomarra Horst are aged c.1775-1750 Ma. Previously dated at 1880-1810 Ma (Beardsmore et al., 1988). The contact between this Group and the Corella/Doherty Formations is associated with Cu/Au mineralisation. This Group hosts numerous IOCG and Broken Hill style mineral deposits. Subject to multiple metamorphic events (described) between 1659-1500 Ma. Seismic sections, magnetic susceptibility, geochemistry discussed. Magnetic and gravity worms discussed.|1675 - 1650 Ma|Maronan Supergroup|Includes Kuridala Formation, Gandry Dam Gneiss, Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Conformably overlain by Corella Formation. Overlies Doherty Formation, conformably overlies Fullarton River Group. Is correlated with Young Australia Group.|Psammo-pelitic rock packages; voluminous mafic volcanics and related sills and dykes in the east.|04-APR-17
26144|Soldiers Cap Group|65755|4|Described|p2, p3 Fig.1|||Quartzite, muscovite and biotite schist, pelitic to psammitic gneiss, and migmatite. Contains Toole Creek Volcanics, Mount Norna Quartzite, Llewellyn Creek Formation in the North; Glen Idol Schist and Gandry Dam Gneiss in the South. 1685 - 1655 Ma.||||||
26144|Soldiers Cap Group|65887|5|Briefly described|p39, p50-53|||In Mount Isa region. Fe-rich tholeiitic intrusives (cf. Etheridge Group) aged c.1670-1650 Ma. Includes Llewellyn Creek Formation, Mount Norna Quartzite and Toole Creek Volcanics.||||||
26144|Soldiers Cap Group|66529|5|Briefly described|p3, p4 Fig.2, p45 |||Eastern part of Mount Isa Province. Affected by sodic and sodic-calcic alteration assemblages.|~1676 Ma (Page and Sun, 1998).||||Deep water turbidites that contain mafic intrusive and extrusive igneous rocks and minor felsic volcanic rocks.|
26144|Soldiers Cap Group|66800|6|Mentioned|p933.|||||Unit in Maronan Supergroup.|Includes Gandry Dam Gneiss.|||
26144|Soldiers Cap Group|66913|5|Briefly described|p170 fig 1, p172, p189||||Deposition 1710-1670 Ma? ||||Includes turbidites, quartzite, basalt, and dolerite.|
26144|Soldiers Cap Group|67323|4|Described|p17-22, p25-26, p34-35, p39, p41|Paleoproterozoic|Paleoproterozoic|See also p71-72, p84, p107, GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin. Informal Lower Soldiers Cap Group used on Solid Geology map. Relatively non-magnetic, but mafic bodies (esp. sills) have moderate to high response. Future studies may consider dropping the dual nomenclature with Kuridala Group. Turbidite succession deposited on a continental slope. Deformed and metamorphosed during the Isan Orogeny between ~1600 and 1500 Ma. In the Soldiers Cap Domain, metamorphic grade increases southwards into gneiss and migmatite. Has Au, Ag, Cu, Pb, Zn, Pb-Zn and IOGC anomalies.|~1685 Ma to ~1650 Ma (max. deposition ages).||Includes Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Probably overlies Staveley Formation. Correlated with Kuridala Group. Is intruded by Toole Creek Volcanics, Williams Supersuite, Maramungee and Cowie Suites.|Gneiss and schist locally migmatitic grading into low-grade metasedimentary rocks; quartzite and psammitic schist; amphibolite grading into metabasalt, metadolerite and metagabbro; minor banded iron formation.|
26144|Soldiers Cap Group|67341|6|Mentioned|vii|||Mount Isa Province.||||||
26144|Soldiers Cap Group|67497|6|Mentioned|p912|Statherian|Statherian|See also Soldiers Cap Formation p913. Age (c.1670 - 1700 Ma) implied in Fig 20.|||||Meta-sedimentary rocks.|07-MAY-12
26144|Soldiers Cap Group|67498|4|Described|p917-918, p924-925, p926, 927, 929-933|Statherian|Statherian|Calvert and Isa Superbasins. Shown as part of 'cover sequence 3'.|1750 - 1739 Ma||Includes Mount Norna Quartzite, Llewellyn Creek Formation.|Intruded by the Wonga Suite and the Williams-Naraku Suite.|Includes deformed metasedimentary successions and interlayered amphibolites. Sodic-calcic alteration occurs in the metasedimentary successions.|08-MAY-12
26144|Soldiers Cap Group|67539|5|Briefly described|p10, p13||Statherian|Replaced by Boomarra Metamorphics in Boomarra Horst area. Extended to include previously undivided Soldiers Cap Group rocks of high metamorphic grade in the SE of the Kuridala and Selwyn sheets. Displays high potassium content in radiometrics images (rich in muscovite).|~ 1690 - 1650 Ma (detrital zircon)||Includes Llewellyn Creek Formation (basal), Mount Norna Quartzite (middle), and Toole Creek Volcanics (upper).|||
26144|Soldiers Cap Group|68021|5|Briefly described|p135 fig 4, p136, 137, 138|Statherian|Statherian|Eastern Succession. Intruded by 1685 Ma variably metamorphosed dolerite, but sediments contain detrital zircons of same age.|~1685 Ma||No lateral or temporal equivalents preserved.||Metamorphosed deep water siliciclastic turbidites intercalated with carbonaceous sediments.|
26144|Soldiers Cap Group|68146|5|Briefly described|p4, p113, p127-128, p201, p203-204|||Interpreted to form the basement immediately underlying the Carpentaria Basin between the Mount Isa and Georgetown Inliers. Dating suggests the three components of this Group cannot be correlated directly with those of the Kuridala Group; only the upper part may be equivalent to the latter. Age determination by Page and Sun (1998).|c.1680-1660 Ma maximum depositional age.||Llewellyn Creek Formation, Toole Creek Volcanics, Mount Norna Quartzite.|||
26144|Soldiers Cap Group|68542|6|Mentioned|p14, p16 fig 4, p18||||1712-1654 Ma|||Correlated with Young Australia Group||
26144|Soldiers Cap Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
26144|Soldiers Cap Group|68576|5|Briefly described|Q_2: p14, p16, p18|||Part of Cover Sequence 3 (1690-1650 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||Lateral facies equivalent of Young Australia Group.||
26144|Soldiers Cap Group|68704|5|Briefly described|p25, p26 Fig.2|||Muscovite-rich.  Displays high potassium content in radiometrics images, distinguished from Squirrel Hills Granite by mineralogy shown in hyperspectral imagery. ||||||
26144|Soldiers Cap Group|68732|5|Briefly described|p158-159, p163-164, p167, p169-171|||Mount Isa Inlier.|||Includes Llewellyn Creek Formation.||A fining-upward siliciclastic succession several kilometres thick.|01-DEC-17
26144|Soldiers Cap Group|69056|4|Described|p2, p4-6, p9, p13, p18, p21, p55, p57|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area. Regionally broad unit in Soldiers Cap and Fig Tree Gully Domains. Contact with Staveley Formation plays a significant role in epigenetic Cu-Au-Fe oxide mineralisation. Is overlain unconformably by the ~3km-thick Millungera Basin sequence.|~1688 - ~1648 Ma.||Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Is intruded by mafic sills: probably Toole Creek Volcanics.||
26144|Soldiers Cap Group|69222|6|Mentioned|p222 Fig.2|Statherian|Statherian|Eastern Fold Belt.||||||
26144|Soldiers Cap Group|69370|4|Described|p305, p307-316.|Statherian|Statherian|c.7.5 km thickness of low-pressure/high-temperature volcano-sedimentary rocks, metamorphosed to greenschist to upper amphibolite facies. Structural deformation discussed in detail.|1685-1655 Ma (Page and Sun, 1998).||Includes Llewellyn Creek Formation, Mount Norna Quartzite and Toole Creek Volcanics.||Mafic intrusives and metasomatitic albitite bodies in lower part; thick interlayered pelitic, psammitic and volcanic units in upper part.|25-JAN-19
26144|Soldiers Cap Group|69582|4|Described|p20-p21, p24-p26, p28-p29|Palaeoproterozoic|Palaeoproterozoic|Eastern Fold Belt Subprovince (Mount Isa Inlier). Underlies the Millungera Basin. Has undergone mutliple phases of deformation and intrusion. An inferred geothermal energy resources is interpreted between 3190-5000m depth in the Millungera Basin.||||Intruded by the Williams Supersuite.|Metasiltstone with graphite, meta-chert, marble, iron formation, quartzite and numerous metadolerite dykes and sills.|
26144|Soldiers Cap Group|69591|5|Briefly described|p29, p41-43, p46, p48, p51, p55, p64|Paleoproterozoic|Paleoproterozoic|See also p67, p69 Fig.2.65, p76, p99, p103, p108. Soldiers Cap Domain, Calvert Superbasin. Geographically separated from the Kuridala Group by a belt of Staveley Formation and Squirrel Hills Granite. Turbiditic deposits on continental slope. Metamorphic grade increases southwards into gneiss and migmatite. Is intruded by some calc-silicate breccias (probably formed by fluidisation from late-Isan Orogeny magmatism) of the Staveley Formation as dyke- and plug-like masses. Strikingly similar to Cobbold Metadolerite (Georgetown Inlier).|||Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Partly equivalent (is adjacent to) the Kuridala Group subsurface.|Includes pelitic and psammitic metasedimentary rocks.|
26144|Soldiers Cap Group|69952|6|Mentioned|p51|||Has previously been correlated with Kuridala Group. These recent geochronological ages cast doubt on that correlation and current understanding of stratigraphic relationships within the Kuridala Group.||||||
26144|Soldiers Cap Group|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|||
26144|Soldiers Cap Group|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|||
26144|Soldiers Cap Group|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Gneiss and schist locally migmatitic grading into low-grade metasedimentary rocks; quartzite and psammitic schist; amphibolite grading into metabasalt, metadolerite and metagabbro; minor BIF.|
26144|Soldiers Cap Group|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.|||Toole Creek Volcanics, Mount Norna Quartzite, Llewellyn Creek Formation|Equivalent to Kuridala Group.|Includes schistose amphibolite, metabasalt and metadolerite; mainly sills.|05-MAY-16
26144|Soldiers Cap Group|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.|||Includes Llewellyn Creek Formation, Mount Norna Quartzite, Toole Creek Volcanics.|Intruded by schistose amphibolite, metabasalt and metadolerite sills.||
26144|Soldiers Cap Group|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.|||Includes Toole Creek Volcanics, Mount Norna Quartzite.|Intruded by unnamed schistose amphibolite, metabasalt and metadolerite.||20-JAN-22
26144|Soldiers Cap Group|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.|||Includes Mount Norma Quartzite, Toole Creek Volcanics.|||
26144|Soldiers Cap Group|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Gneiss and schist locally migmatitic grading into low grade metasediments; quartzite and psammitic schist; amphibolite grading into metabasalt, metadolerite and metagabbro; minor banded iron formation.|
26144|Soldiers Cap Group|71382|5|Briefly described|p8|Palaeoproterozoic|Palaeoproterozoic|Eastern Mount Isa Inlier. Outcrops to the west of the Millungera Basin. Equivalent to the basement of the Millungera Basin. Undergone multiple phases of deformation and intrusion.||||Intruded by the Williams Supersuite.|Metasiltstone with possible graphite, meta-chert, marble, iron formation, metabasalt, quartzite units and numerous metadolerite dykes and sills.|
26144|Soldiers Cap Group|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1654+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Felsic volcanics.|
26144|Soldiers Cap Group|71799|5|Briefly described|p150 fig 2, p154, p155, p160|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca 1700 Ma|||Overlain by the Toole Creek Volcanics.|Sandstone and greywacke.|
26144|Soldiers Cap Group|72297|6|Mentioned|p732, p757|Proterozoic|Proterozoic|Muscovite mica was extracted from this unit 26km N of Cannington homestead. Red garnets occur on Maronan station, NW QLD.||||||
26144|Soldiers Cap Group|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1656 +/- 5 Ma|||||
26144|Soldiers Cap Group|72889|5|Briefly described|p2, p4-p6, p33, p35.||||||Includes Llewellyn Creek Formation, Mount Norna Quartzite|Laterally equivalent to the Kuridala Group.||25-NOV-20
26144|Soldiers Cap Group|73137|6|Mentioned|p76|||||||||
26144|Soldiers Cap Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Eastern Fold Belt.||||||
26144|Soldiers Cap Group|73527|6|Mentioned|p9|Statherian|Statherian|Mount Isa Inlier, eastern.|1700-1650 Ma|||||
26144|Soldiers Cap Group|73529|6|Mentioned|p16 Fig.12|||||||||
26144|Soldiers Cap Group|73553|6|Mentioned|p29, p177 Tb.5.9.2|||Contains concordant folded mafic sills, metamorphosed.||||||
24498|Sonoma Member|40247|5|Briefly described|p211|||||||||
24498|Sonoma Member|40954|6|Mentioned|p133|||||||||
24498|Sonoma Member|42975|6|Mentioned|Fig.2 p257|||of Lowmead Formation||||||
24498|Sonoma Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably underlain by the Makowata Oil Shale Member.|Dominantly olive-grey claystone, interbedded with carbonaceous oil shale, oil shale and minor sandstone.|
24498|Sonoma Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. Over 296.6m thick.||Lowmead Formation.||Overlies Makowata Oil Shale Member.|Interbedded claystone, oil shale, carbonaceous oil shale, sandstone and siltstone.|
39585|South Buaraba Microdiorite|23799|5|Briefly described|p93, p12 Tb. 1|Middle Triassic|Early Triassic|For full description - see "South Buaraba Microdiorite".  Intrudes the Champion Hills Diorite and Cressbrook Cr. Gp.; intruded by Buaraba Granodiorite.  Unconformably overlain by Woogaroo Subgroup.  Of the SE Queensland Volcanic and Plutonic Intrusives.||||||
39585|South Buaraba Microdiorite|68679|5|Briefly described|p414|||McCabe (1982). West of the Esk Basin, northern New England Orogen.|||||Grey porphyritic diorite.|
41796|South Creek Quartz Diorite|60480|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Biotite-clinopyroxene-hornblende quartz diorite.||||||
41796|South Creek Quartz Diorite|61035|4|Described|p9 Tb. 1|Early Permian|Late Carboniferous|Intrudes Leura Volcanics + Macksford Andesite; unconformably overlain by Coppermine Andesite. Age: 304+/-4Ma (G. Birch, SHRIMP). Geological Province: Connors Sudprovince. Biotite-clinopyroxene-hornblende quartz diorite.||||||07-FEB-11
41796|South Creek Quartz Diorite|65388|2|Defined|p358-359, p86, Fig. 35, p394, 399|Early Permian|Late Carboniferous|Connors Province. Intrudes Leura Volcanics, Macksford Volcanics. Unconformably overlain by Coppermine Andesite. U-Pb SHRIMP age 304+/- 2.2Ma (Burch 1999), but may be up to 8 Ma younger than this. Mainly  grey, fine to medium-grained quartz diorite, and locally porphyritic microdiorite. ||||||
41796|South Creek Quartz Diorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Diorite.|
26145|South Curra Limestone|23251|5|Briefly described|Table 1 p12, p20, p36|Late Permian|Permian|Various shell fossil assemblages of Late Permian age. Of Gympie Group. Kin Kin Subprovince, Gympie Province. Overlying unit Tamaree Formation. Underlying unit Rammutt Formation.||||||21-JUN-06
26145|South Curra Limestone|23542|4|Described|Table 1 p379.|||Of the Gympie Group.||||||22-OCT-08
26145|South Curra Limestone|23799|5|Briefly described|p33|Permian|Permian|Probable correlative of Biarraville Formation.||||||
26145|South Curra Limestone|24078|5|Briefly described|p425 Tb. 1|Early Permian|Early Permian|Bioclastic calcarenite, fine calcareous siltstone near base to coarser more calcareous sediment near top.   Max. thickness: 140m.  Geological Province: Gympie Basin.||||||
26145|South Curra Limestone|29437|6|Mentioned|p136|||Permian||||||
26145|South Curra Limestone|29440|6|Mentioned|p38|||Permian brachiopods||||||
26145|South Curra Limestone|30449|6|Mentioned|p6|||Brachiopods||||||
26145|South Curra Limestone|30450|6|Mentioned|Table 1|||Permian age. Maryborough Basin||||||
26145|South Curra Limestone|31703|5|Briefly described|p3|||||||||
26145|South Curra Limestone|32945|6|Mentioned|p78|||See also PP88,89 & 90. Perm.||||||
26145|South Curra Limestone|33436|6|Mentioned|p241|||Fauna.||||||
26145|South Curra Limestone|33711|6|Mentioned|p384|||||||||
26145|South Curra Limestone|34475|2|Defined|p256|Late Permian|Late Permian|See also pp251,252 etc.||||||28-FEB-19
26145|South Curra Limestone|35008|5|Briefly described|p176|||||||||
26145|South Curra Limestone|35101|5|Briefly described|p31|||||||||
26145|South Curra Limestone|35284|6|Mentioned|p43|||||||||
26145|South Curra Limestone|36045|6|Mentioned|p332|||||||||
26145|South Curra Limestone|36926|6|Mentioned|p168|||||||||
26145|South Curra Limestone|37756|6|Mentioned|p73|||||||||
26145|South Curra Limestone|39252|6|Mentioned|p22|||See also Fig.13||||||
26145|South Curra Limestone|39261|6|Mentioned|p112|||||||||
26145|South Curra Limestone|39262|6|Mentioned|p122|||||||||
26145|South Curra Limestone|39284|5|Briefly described|p431|||||||||
26145|South Curra Limestone|39445|5|Briefly described|Table 8|||||||||
26145|South Curra Limestone|41157|6|Mentioned|Fig.1|||||||||
26145|South Curra Limestone|41736|6|Mentioned|p119|||||||||
26145|South Curra Limestone|41917|6|Mentioned|p526|||||||||
26145|South Curra Limestone|42450|5|Briefly described|p404|||||||||
26145|South Curra Limestone|42751|4|Described|p24|||of Gympie Group||||||
26145|South Curra Limestone|43017|5|Briefly described|Fig.3,p375|||||||||
26145|South Curra Limestone|43018|6|Mentioned|p392|||||||||
26145|South Curra Limestone|43100|4|Described|p25|||of Gympie Group.||||||22-OCT-08
26145|South Curra Limestone|44928|5|Briefly described|Map Legend||Permian|||||||
26145|South Curra Limestone|45440|14|Not recorded|p.13|||||||||
26145|South Curra Limestone|61780|4|Described|p258|Late Permian|Middle Permian|Thickness: 60-150m. Sparry bioclastic limestone, carbonaceous, silty micritic limestone and calcarenite (shallow marine-lagoonal; restricted circulation).||||||
26145|South Curra Limestone|65380|5|Briefly described|p671|Kungurian|Artinskian|Includes ammonite described and dated from Elderslie Formation, Sydney Basin. ||||Overlies Rammutt Formation.||
26145|South Curra Limestone|68679|5|Briefly described|p369-370, p386|Permian|Permian|Runnegar and Ferguson (1969). Southern Gympie Province. 60-150m thick. Contains a prolific fauna; mostly Kungurian.||Gympie Group.||Is overlain by the Tamaree Formation. Correlated with Gigoomgan Limestone. May correlate with Biarraville Formation (Cressbrook Basin).|Silty, sandy and muddy limestone, minor sparry limestone. Distinctive widespread sandstone marker within 20m of the top of the limestone with lithic grains and abundant shell fragments.|
26145|South Curra Limestone|70913|1|Redefined|p1, p2, p9, p17-p20, p23, App 1 maps|Middle Permian|Middle Permian|Gympie Province. Name derived from the Curra Siding, northwest of Gympie. Usage not modified here. Type section briefly described and a drill section is mentioned. Thickness in the type section is around 130m and underground the thickness is between 80-120m thick.  Distribution and Middle Permian fossil assemblages are discussed. Note that the U-Pb age is from 'an interstratified tuff layer' but may be contentious due to a faulted contact near where this sample was derived. Deposited in a low energy, restricted marine environment. See also p7, p8, p67 fig 9, p76, p77, p79. See also Curra Limestone p12.|258.3 +/- 2.6 Ma (U-Pb zircon, Li et al, 2015)|Gympie Group|Shown as including the Langton Dolerite.|Apparently conformably overlies the Glanmire Conglomerate Member of the Rammutt Formation. Where base is not faulted, conformably overlain by the Tamaree Formation.|Calcareous siltstone grading upwards into dominant coarse grained bioclastic calcarenite, calcilutite and fossil-free limestone. Interbedded siltstones are also present.|28-FEB-19
26145|South Curra Limestone|72037|4|Described|p859,861-863,865-866,870|Late Permian|Middle Permian|Geological province: New England Orogen, Gympie Terrane. Depositional environment: shallow marine to lagoonal. La-ICP-MS peak detrital zircon U-Th-Pb age at 258.3+\-2.6 Ma from an interstratified tuff layer in the upper part of the unit. Age constraints for the lower part of the unit provided the the Neocrimites meridionalis ammonite assemblage, and by SHRIMP zircons ages of 272+\-3 Ma and 264+\-2 Ma from tuffaceous sandstones in the Sydney Basin above and below a similar fossiliferous horizon. ||||Overlain conformably by Tamaree Formation. Underlain conformably by Rammutt Formation.|Impure bioclastic limestone, calcarenite, and minor volcanic rocks.|
26145|South Curra Limestone|73303|5|Briefly described|p61 Fig.2, p62, p65 Fig.5, p69-70|Lopingian|Cisuralian|New England Orogen. Gympie Terrane, southern. 258 Ma volcanic zircon maximum depositional age from upper part of unit. Brachiopod fauna assemblage equivalent to Gigoomgan Limestone. Shallow marine/lagoonal depositional environment.|265 Ma detrital zircon maximum depositional age|||Overlies Rammutt Formation, underlies Tamaree Formation|Calc-arenite limestone.|
36417|South Island Gabbro|23617|4|Described|Table 2 p18|Permian|Late Carboniferous|Also see p30. This name is proposed for gabbro-forming South Island, at the southern end of the Brook Islands group. Kennedy Province.||||||
36417|South Island Gabbro|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36417|South Island Gabbro|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
25486|South Kolan Nephelinite|42895|3|Fully described|p62|||age of 5.1 Ma||||||
25486|South Kolan Nephelinite|68332|5|Briefly described|Map legend.|Neogene|Neogene|Bundaberg Volcanic Province.|5.1 Ma K/Ar ; 4.54 +/- 0.09 Ma Ar/Ar.||||Olivine nephelinite.|26-MAR-15
75137|South Mission granite|60425|5|Briefly described|p62 Tb. 4|Late Ordovician|Ordovician|Informally named subunit of Mission Beach Granite Complex. I-type.||||||07-FEB-11
23981|Southern Cross Formation|22713|5|Briefly described|p125|Paleocene|Paleocene|||||||
23981|Southern Cross Formation|22937|5|Briefly described|p203 fig1|Tertiary|Tertiary|||||||
23981|Southern Cross Formation|23082|5|Briefly described|p686||Tertiary|||||||
23981|Southern Cross Formation|23422|4|Described|p186, p204 Table 6.3|Early Eocene|Paleocene|Overlying unit: Nulla Basalt.||||||
23981|Southern Cross Formation|23430|5|Briefly described|p504 Table 14.5|||Also see p527. Kalpowar Basin Province.||||||
23981|Southern Cross Formation|23431|5|Briefly described|p538|||||||||
23981|Southern Cross Formation|23504|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
23981|Southern Cross Formation|23505|5|Briefly described|Map legend||Tertiary|||||||
23981|Southern Cross Formation|23893|5|Briefly described|p22|Cenozoic|Cenozoic|||||||19-NOV-08
23981|Southern Cross Formation|23986|4|Described|p89|||Geological Province: Drummond Basin.||||||
23981|Southern Cross Formation|23987|5|Briefly described|p1|||||||||
23981|Southern Cross Formation|23988|4|Described|p10|||See also page 42.||||||
23981|Southern Cross Formation|24031|6|Mentioned|p2|||Equivalent to Suttor Formation.||||||
23981|Southern Cross Formation|24036|5|Briefly described|p2, p3 Fig. 1|Tertiary|Tertiary|Overlies Paleozoic basement rocks. Geological Province: North Drummond Basin. Sedimentary rocks and generally clay-rich.||||||
23981|Southern Cross Formation|37607|5|Briefly described|p336|||See also Fig.7||||||
23981|Southern Cross Formation|39445|5|Briefly described|Table 14|||Eocene. See also P150||||||
23981|Southern Cross Formation|39686|6|Mentioned|p74|||||||||
23981|Southern Cross Formation|39735|6|Mentioned|p19|||||||||
23981|Southern Cross Formation|41774|6|Mentioned|p33|||||||||
23981|Southern Cross Formation|41805|6|Mentioned|p29|||||||||
23981|Southern Cross Formation|43687|5|Briefly described|p203|||||||||
23981|Southern Cross Formation|43934|6|Mentioned|Map Legend||Tertiary|||||||
23981|Southern Cross Formation|43936|6|Mentioned|Map legend|Tertiary|Tertiary|Mentioned in description of Tertiary unit Ts.||||||
23981|Southern Cross Formation|46902|6|Mentioned|p42|||||||||
23981|Southern Cross Formation|50153|5|Briefly described|p1,4,9,12-15, 20-24|Paleocene|Cenozoic|Correlated with the Suttor Formation to the south. Older than Campaspe Formation. May have widespread subsurface distribution.|||||Dominantly fluviatile and lacustrine sandstones and siltstones.|
23981|Southern Cross Formation|60659|6|Mentioned|p54|Tertiary|Tertiary|||||||07-FEB-11
23981|Southern Cross Formation|61155|5|Briefly described|p20|Middle Eocene|Middle Eocene|Thickness: 15m. In the Townsville area.||||||
23981|Southern Cross Formation|61814|5|Briefly described|p18|Tertiary|Tertiary|Forms an extensive blanket over the Drummond Basin and the Lolworth-Ravenswood Block. Partly overlain by the Campaspe Formation. Age is Midlde Tertiary.||||||08-FEB-10
23981|Southern Cross Formation|61829|5|Briefly described|p174, p175, p176|Cenozoic|Cenozoic|Weathered sandy gravel to sandy clay sediments; includes red palaeosols.||||||09-JUN-06
23981|Southern Cross Formation|61835|5|Briefly described|p193, p194, p196|Tertiary|Tertiary|Max. thickness: <80m.  Geological Province: Drummond Basin.||||||03-JUL-06
23981|Southern Cross Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
23981|Southern Cross Formation|69599|5|Briefly described|p580, p584-585, p593|Oligocene|Paleocene|Charters Towers and northern Drummond Basin. Forms perched remnants or cappings on uplands. Fluvial or lacustrine deposits with possible colluvial inputs. Age discussed. Silcrete and ferricrete development (Featherby Surface) occurred in late Eocene-Oligocene.||||Correlated with Biloela beds; Exevale, Suttor, Emerald and Duarings Formations.|Sandstone, pebbly sandstone and minor siltstone. Deeply weathered; has a significant ferricrete surface.|
23981|Southern Cross Formation|69789|5|Briefly described|p1042, p1044-1046, p1051-1053, p1056|Paleogene|Paleogene|Fluviatile-lacustrine deposits. Has undergone intense leaching, developing a ferricrete duricrust surface, erosional remnants of which are prominent in the landscape. Likely source of sediment for Campaspe Formation.||||Is overlain disconformably by Campaspe Formation. Also shown as underlying Allingham Formation.||22-JUN-20
23981|Southern Cross Formation|73115|6|Mentioned|p25, p80|||Nulla Basalt Province. Represents sedimentation in sub-distal to distal zones.||||Overlain by Campaspe Formation.||
27570|Spanner Limestone Member|23032|5|Briefly described|p28 fig6|Devonian|Devonian|||||||
27570|Spanner Limestone Member|23424|5|Briefly described|Table 8.1 p336|Givetian|Emsian|Of Papilio Mudstone/Wando Vale Subgroup, Graveyard Creek Subprovince.||||||21-JUN-13
27570|Spanner Limestone Member|23522|5|Briefly described|p250 Fig 6|Givetian|Givetian|||||||
27570|Spanner Limestone Member|41260|3|Fully described|p70|||Described Table 1. Reserved as Spanner Limestone||||||
27570|Spanner Limestone Member|41679|2|Defined|p260|Givetian||||||||
27570|Spanner Limestone Member|41719|6|Mentioned|Fig.2|||||||||
27570|Spanner Limestone Member|41739|6|Mentioned|Fig.2|||||||||
27570|Spanner Limestone Member|42031|5|Briefly described|Fig.5 P762|||||||||
27570|Spanner Limestone Member|42032|6|Mentioned|Fig.12 P505|||||||||
27570|Spanner Limestone Member|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
27570|Spanner Limestone Member|42933|3|Fully described|Table 2|||See also p112. Of Papilio Mudstone.||||||
27570|Spanner Limestone Member|50093|6|Mentioned|p329 Fig.2|Givetian|Givetian|Of Broken River Group.||||||07-FEB-11
27570|Spanner Limestone Member|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27570|Spanner Limestone Member|68336|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Papilio Mudstone.|||Nodular, bioclastic limestone (calcarenite, calcirudite and calcilutite); minor calcareous sandstone and mudstone.|
27570|Spanner Limestone Member|68341|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Papilio Mudstone.|||Nodular, bioclastic limestone (calcarenite, calcirudite and calcilutite); minor calcareous sandstone and mudstone.|
27570|Spanner Limestone Member|68478|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Papilio Mudstone.|||Nodular, bioclastic limestone (calcarenite, calcirudite, and calcilutite); minor calcareous sandstone and mudstone.|
27570|Spanner Limestone Member|68479|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Papilio Mudstone.|||Nodular, bioclastic limestone (calcarenite, calcirudite, and calcilutite); minor calcareous sandstone and mudstone.|
27570|Spanner Limestone Member|69592|6|Mentioned|p264|||||||||
36633|Spear Creek gabbro|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 489.||||||
36174|Specimen Hill Granite|23506|5|Briefly described|Map Legend||Early Permian|of O'Briens Creek Supersuite.||||||
36174|Specimen Hill Granite|60425|4|Described|p284-5 Appdx.|Early Permian|Early Permian|Of Cherry Tree Suite (O'Briens Creek Supersuite). Detailed lithology included (biotite granite, minor microgranite). I-type. Delineated as a discrete unit by Clarke (1990, 1995); included in Saint Patrick Hill Granite by Donchak and Bultitude (1998).||||||07-FEB-11
22877|Spider Gully Granodiorite|22847|3|Fully described|p 55|Early Devonian|Late Silurian|||||||
22877|Spider Gully Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22877|Spider Gully Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 207. I-Type.||||||
22877|Spider Gully Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
22877|Spider Gully Granodiorite|43259|4|Described|Appendix 1,p30.|Early Devonian|Late Silurian|||||||
22877|Spider Gully Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
22877|Spider Gully Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
27057|Spinifex Creek Granite|23422|6|Mentioned|p181|||See also Spinifex Granite.||||||
27057|Spinifex Creek Granite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
27057|Spinifex Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 134. I-Type.||||||
27057|Spinifex Creek Granite|23893|6|Mentioned|p28|||See also Spinifex Granite.||||||
27057|Spinifex Creek Granite|24613|6|Mentioned|p109|Carboniferous|Carboniferous|||||||07-FEB-11
27057|Spinifex Creek Granite|42689|5|Briefly described|map legend|Carboniferous||||||||
27057|Spinifex Creek Granite|42690|5|Briefly described|map legend|Carboniferous||||||||
27057|Spinifex Creek Granite|42692|5|Briefly described|map legend|Carboniferous||||||||
27057|Spinifex Creek Granite|43095|3|Fully described|p49||Carboniferous|Probable Carboniferous age.||||||22-APR-08
27057|Spinifex Creek Granite|43259|4|Described|Appendix 1,p25.||Carboniferous|||||||
27057|Spinifex Creek Granite|43589|2|Defined|p21|Early Carboniferous|Early Carboniferous|This granite and Macauley Creek Granite were previously mapped as Oweenee Granite by Wyatt and others (1970).||||||15-MAY-15
27057|Spinifex Creek Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Cream to pink, medium- to coarse-grained, equigranular to porphyritic biotite granite, minor microgranite, aplite and local greisen; pink to cream, equigranular microgranite, locally silicified and altered.|
27057|Spinifex Creek Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Cream to pink, medium- to coarse-grained, equigranular to porphyritic biotite granite, minor microgranite, aplite and local greisen; pink to cream, equigranular microgranite, locally silicified and altered.|
27057|Spinifex Creek Granite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Macauley Creek Granite and is intruded by the Coane Range Granite Complex.|Cream to pink, medium to coarse-grained, equigranular to porphyritic biotite granite; minor microgranite and aplite and local greisen.|
27057|Spinifex Creek Granite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Oweenee Batholith, Kennedy Province.||||Intrudes Macauley Creek Granite and is intruded by Coane Range Granite Complex.|Cream to pink, medium to coarse-grained, equigranular to porphyritic biotite granite; minor microgranite and aplite and local greisen.|
83360|Spion Kop rhyolite|72983|5|Briefly described|p7, p46-50|Kungurian|Artinskian|Informal unit name. Kennedy Igneous Association. Cape York region. Yarraden Goldfield. Constitutes a locally brecciated rhyolite plug; polymict clasts include unidentified granite. Breccia associated with Au arsenopyrite and pyrite mineralisation. Age provides the first reliable maximum age constraint for gold mineralisation in the southernmost part of the Yarraden Goldfield. Age is within uncertainty of that of Wolverton Granite.|281.5 +/- 3.9 Ma SHRIMP U-Pb|||Intrudes[?] Flyspeck Granodiorite.|Rhyolite.|
23985|Spondulix Granodiorite|22847|3|Fully described|p 51|Early Devonian|Late Silurian|||||||
23985|Spondulix Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23985|Spondulix Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 122. I-Type.||||||
23985|Spondulix Granodiorite|42245|2|Defined|p38|Early Devonian|Late Silurian|||||||
23985|Spondulix Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
23985|Spondulix Granodiorite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|||||||
23985|Spondulix Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23985|Spondulix Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Spondulix gdrt.||Unit in Millchester Supersuite.||||
78956|Spring Valley Quartz Monzonite|65388|6|Mentioned|p394|||Northern Connors Range map sheet.||||||
82146|Springlands Gabbro|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, fine to medium-grained, uneven-grained to slightly porphyritic gabbro, quartz gabbro; with various proportions of augite, hypersthene, hornblende, biotite and quartz; mainly massive but with a weak foliation locally.|
82146|Springlands Gabbro|73036|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, fine to medium-grained, uneven-grained to slightly porphyritic gabbro, quartz gabbro; with various proportions of augite, hypersthene, hornblende, biotite and quartz; mainly massive but with a weak foliation locally.|
26907|Springvale Formation|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26907|Springvale Formation|37607|6|Mentioned|p332|||See also Fig.4.||||||
26907|Springvale Formation|39445|5|Briefly described|Table 14|||||||||
26907|Springvale Formation|44087|14|Not recorded|p8,9,opp.7||Tertiary|||||||
26907|Springvale Formation|44090|14|Not recorded|Map Legend||Tertiary|||||||
26907|Springvale Formation|44122|14|Not recorded|Fig.48,321|||||||||
26907|Springvale Formation|44133|5|Briefly described|p190 Fig. 10.30|Miocene|Miocene|||||||
26907|Springvale Formation|44222|14|Not recorded|p.120,121|||||||||
26907|Springvale Formation|44291|2|Defined|Tb.1,opp.p6,9,10,13|||Probably contemporary with Marion Formation. Map.||||||
26907|Springvale Formation|44313|14|Not recorded|Map Legend||Tertiary|||||||
26907|Springvale Formation|44351|2|Defined|p2-10,15,20-23,||Tertiary|Pls.1-5,9,Fig.13. Overlain by Horse Creek Formation. Overlies Moses Sandstone. (Tertiary-Cenomanian or younger)||||||
26907|Springvale Formation|44413|14|Not recorded|p470-471|||Overlies Moses Sandstone.||||||
26907|Springvale Formation|44543|2|Defined|p35,36||Cenozoic|Overlies Wilgunya Formation. Probably same age as Noranside and Austral Downs Limestone. (Late Tertiary or Quaternary)||||||19-NOV-08
26907|Springvale Formation|44836|14|Not recorded|p11,238,Fig.5||Tertiary|||||||
26907|Springvale Formation|45145|6|Mentioned|Table 7|||||||||
26907|Springvale Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
26907|Springvale Formation|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Geological region: Diamantina.||||||
26907|Springvale Formation|63450|6|Mentioned|p83|Cenozoic|Cenozoic|Geological province: Georgina Basin.||||||07-FEB-11
26907|Springvale Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Middle Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
26907|Springvale Formation|67323|5|Briefly described|solid geol.||||||||Ferruginised and silicified lacustrine limestone, claystone, clayey sandstone; ?unconformable on Moses Sandstone|
26907|Springvale Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
26907|Springvale Formation|69599|5|Briefly described|p584, p599, p651|Eocene|Paleocene|Springvale Basin. Up to 22m thick. Contains freshwater gastropods and indeterminate algae. Capped by silcrete and laterite of the Canaway profile. RELATED UNITS (continued): Also correlated (at least partly) with Eyre, Glendower, Edkins, Moonie and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.||||Unconformably overlies Moses Sandstone. Is overlain unconformably by the Horse Creek Formation. See COMMENTS for more.|Limestone, sandstone and mudstone; extensive silcretisation.|
36735|Spurgeon Granite|23423|5|Briefly described|p284|||S-type||||||
36735|Spurgeon Granite|60425|4|Described|p189, p274-5 Appdx. 1|Early Permian|Early Permian|Of Mount Carbine Suite (Whypalla S'suite). S-type.Outer fine-grained porphyritic zone grading into a central, more even-grained, medium-grained zone; host to large to small tourmaline-rich quartz and quartz-feldspar veins. Detailed lithology on p275||||||07-FEB-11
36735|Spurgeon Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Mount Carbine Suite.||||
23986|Spyglass Andesite Member|23291|4|Described|p37, p81 Tb. 3.6|Carboniferous|Devonian|Parent: Gilberton Formation. Geological Province: Georgetown Region.||||||19-MAY-15
23986|Spyglass Andesite Member|23430|5|Briefly described|p509|||Of Gilberton Formation. Gilberton Basin Province.||||||
23986|Spyglass Andesite Member|23513|5|Briefly described|Map legend|Carboniferous|Devonian|Palaeozoic Volcanic No. V10. I-Type.||||||
23986|Spyglass Andesite Member|39917|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian-Early Carboniferous||||||
23986|Spyglass Andesite Member|40542|6|Mentioned|p97|||||||||
23986|Spyglass Andesite Member|43259|4|Described|Appendix 1,p2.|Early Carboniferous|Late Devonian|Part of the Gilbert Formation.||||||
23986|Spyglass Andesite Member|50595|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Gilberton Formation.||||||
23986|Spyglass Andesite Member|68352|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Gilberton Basin.||Unit in Gilberton Formation.|||Greenish grey, sparsely porphyritic (and extensively altered) andesite.|
23986|Spyglass Andesite Member|69591|5|Briefly described|p103|||Dismal Creek area.||Gilberton Formation.|||Extensively altered andesitic lavas.|
77807|Square Rock Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Biotite granite to leucogranite.|
24501|Squirrel Hills Granite|22465|6|Mentioned|p934|||||||||
24501|Squirrel Hills Granite|22515|3|Fully described|Fig1p398,402-3,407||Paleoproterozoic|||||||07-NOV-08
24501|Squirrel Hills Granite|22667|6|Mentioned|Fig1 P234|||||||||
24501|Squirrel Hills Granite|22735|6|Mentioned|p282 Fig 1|Calymmian|Calymmian|spelled with informal lower case (incorrect) g in figure 1 caption/key||||||
24501|Squirrel Hills Granite|23069|5|Briefly described|p775 (fig 1)|||||||||
24501|Squirrel Hills Granite|23333|5|Briefly described|1116 Fig.3|||||||||
24501|Squirrel Hills Granite|23471|5|Briefly described|p110 Fig 1|Calymmian|Calymmian|Age: 1514+/-4 Ma and 1511+/-9 Ma (U-Pb SHRIMP). Geological Province: Mount Isa Block.||||||
24501|Squirrel Hills Granite|23519|5|Briefly described|p128|Proterozoic|Proterozoic|See also page 106 Fig 1. Age: ~1493-1508 Ma. Geological Province: Williams Batholith.||||||
24501|Squirrel Hills Granite|23545|5|Briefly described|p606 Table 1.|||||||||
24501|Squirrel Hills Granite|23563|6|Mentioned|p215 Fig 1|||See also p234: SHRIMP analysis of U/Pb in zircon yields ages of 1514+/-5 and 1511+/-9 Ma for two samples from the Lightning creek plutonic suite (Pollard and McNaughton, unpublished data). [unclear if these samples were Squirrel Hills pluton, but it seems likely]||||||19-MAR-18
24501|Squirrel Hills Granite|23920|6|Mentioned|p1068|||Geological Province: Eastern Fold Belt.||||||
24501|Squirrel Hills Granite|23967|5|Briefly described|p1334|||||||||
24501|Squirrel Hills Granite|23974|6|Mentioned|p1452 Fig. 2a|||Geological Province: Selwyn Region.||||||
24501|Squirrel Hills Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24501|Squirrel Hills Granite|24254|6|Mentioned|p17 Fig.1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
24501|Squirrel Hills Granite|24256|6|Mentioned|p48, p50 Fig.2|||Geological Province: Mount Isa Block.||||||
24501|Squirrel Hills Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
24501|Squirrel Hills Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
24501|Squirrel Hills Granite|37862|4|Described|p589|||||||||
24501|Squirrel Hills Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24501|Squirrel Hills Granite|38658|6|Mentioned|p153|||||||||
24501|Squirrel Hills Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24501|Squirrel Hills Granite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24501|Squirrel Hills Granite|39445|6|Mentioned|Table 2|||||||||
24501|Squirrel Hills Granite|39496|4|Described|p15|||||||||
24501|Squirrel Hills Granite|40840|6|Mentioned|Map legend|||||||||
24501|Squirrel Hills Granite|41306|6|Mentioned|p4|||||||||
24501|Squirrel Hills Granite|42556|6|Mentioned|p10|||||||||
24501|Squirrel Hills Granite|43490|6|Mentioned|8|||||||||
24501|Squirrel Hills Granite|45161|5|Briefly described|p52|||||||||
24501|Squirrel Hills Granite|45166|5|Briefly described|p39|||||||||
24501|Squirrel Hills Granite|49009|2|Defined|p42|Proterozoic|Proterozoic|Mapped as part of the Williams Granite (Carter & Opik,1963).||||||
24501|Squirrel Hills Granite|50100|5|Briefly described|p21, p74|Calymmian|Calymmian|Of the Williams Supersuite.||||||
24501|Squirrel Hills Granite|50536|5|Briefly described|p1.5, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite.||||||
24501|Squirrel Hills Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
24501|Squirrel Hills Granite|60658|6|Mentioned|p61|||Granite pluton. Geological Province: Eastern Fold Belt / Mount Isa Inlier||||||15-MAR-07
24501|Squirrel Hills Granite|61927|5|Briefly described|p96|Mesoproterozoic|Mesoproterozoic|Intrusive. Part of the Williams Batholith, various ages of which are between 1530 and 1480 Ma.||||||
24501|Squirrel Hills Granite|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Pluton of the Williams and Naraku Batholiths. Age: 1516-1490 Ma.||||||
24501|Squirrel Hills Granite|61936|5|Briefly described|p200, p203|||A-type, metaluminous, magnetite-bearing plutonic rocks of the Isan Orogeny. Contains the intrusion-hosted Fe-oxide deposits of the Lightening Creek prospect. ||||||
24501|Squirrel Hills Granite|62047|6|Mentioned|p90 Fig.1 |||||||||
24501|Squirrel Hills Granite|64248|6|Mentioned|p33 Fig.1, p45|||A composite intrusion, containing several discrete intrusions that may have approximately internal concentric zones and a wide range of compositions.||||||
24501|Squirrel Hills Granite|64250|6|Mentioned|p10 fig 2|||||||||
24501|Squirrel Hills Granite|64251|5|Briefly described|p55, p60, p61 Fig. 7, p63 Fig. 10, p64|||In contact with Doherty Formation. Geological Province: Mount Isa Inlier.||||||05-MAY-09
24501|Squirrel Hills Granite|65396|5|Briefly described|p4, p22, p40, p53, p56, p61, p172-173|Calymmian|Calymmian|See also p179-180, p213, p224, p272, p276, p279-280, p284, p327, p360-361, p365-368, p438, p440, p445, p474-500. Composite body: several discrete intrusions. Magnetic and gravity worms discussed. Appears as Squirrell Hills Granite on p179, Squirrel Hill Granite on p327, Squirrel Hills granite on p360-361, and as Squirrel hills granite on p276 and p279. Fluid inclusions studied. Stress partitioning and fluid flow models detailed.|1511 +/- 9 Ma, 1514 +/- 5 Ma (SHRIMP)||||Monzodiorite, monzogranite.|19-MAR-18
24501|Squirrel Hills Granite|65755|5|Briefly described|p3|||1510 - 1490 Ma||||||
24501|Squirrel Hills Granite|66913|5|Briefly described|p169-171 fig 2, 176, 187, 189, 190|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2. Hosts hydrothermal magnetite body.||||||
24501|Squirrel Hills Granite|67323|4|Described|GIS attrib tbl, p19-20|Mesoproterozoic|Mesoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Forms the eastern outcrop margin of the Kuridala-Selwyn Domain. Williams Igneous Event. Largest batholith in the Williams Supersuite: forms a batholith 60 x 25 km. Strong magnetic response; low gravity response.|1514 +/- 5 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.||Separates Kuridala Group from Staveley Formation.|Non-porphyritic to porphyritic biotite and hornblende-biotite granite; minor aplite and pyroxene-bearing granite. I-type.|
24501|Squirrel Hills Granite|67498|6|Mentioned|p918 Fig.1, p919, p934|||Hosts magnetite-rich mineralisation.||Of the Williams-Naraku Suite.|||Magmatic-hydrothermal magnetite-rich mineralisation occurs within the Squirrel Hills Granite.|
24501|Squirrel Hills Granite|68542|6|Mentioned|p18|||||||||
24501|Squirrel Hills Granite|68576|6|Mentioned|Q_2: p16, p18|||An intrusive phase of the 1545-1500 Ma Williams/Naraku Batholith, S of Cloncurry.||||||
24501|Squirrel Hills Granite|68704|5|Briefly described|p25, p26 Fig.2|||Feldspar-rich. Displays high potassium content in radiometrics images, distinguished from Soldiers Cap Group by mineralogy shown in hyperspectral imagery |||||Rich in feldspar.|
24501|Squirrel Hills Granite|69056|6|Mentioned|Time-Space plot sheet|Calymmian|Calymmian||1515 +/- 5 Ma SHRIMP age..|||||19-MAR-18
24501|Squirrel Hills Granite|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene-bearing granite and aplite|
24501|Squirrel Hills Granite|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene-bearing granite and aplite|
24501|Squirrel Hills Granite|69591|5|Briefly described|p41, p51, p59|||Geographically separates Kuridala and Soldiers Cap Groups.|1514 +/- 5 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.||||
24501|Squirrel Hills Granite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Squirrel Hills Suite.|||Equigranular to porphyritic biotite and hornblende-biotite granite; minor aplite and pyroxene-bearing granite. (Separately mapped) porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene-bearing granite and aplite.|05-MAY-16
24501|Squirrel Hills Granite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes one unnamed member of porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene bearing granite and aplite.||Squirrel Hills Suite.|Includes one unnamed member.||Equigranular to porphyritic biotite and hornblende biotite granite; minor aplite and pyroxene bearing granite.
|
24501|Squirrel Hills Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Squirrel Hills Suite|||Equigranular to porphyritic biotite and hornblende-biotite granite; minor aplite and pyroxene bearing granite. Porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene bearing granite and aplite.|20-JAN-22
24501|Squirrel Hills Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Squirrel Hills Suite|||Equigranular-porphyritic biotite and hornblende-biotite granite; minor aplite and pyroxene bearing granite. Porphyritic biotite and hornblende biotite granite; minor equigranular granite, pyroxene bearing granite and aplite.|
24501|Squirrel Hills Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1511+/-9 Ma (U-Pb zircon SHRIMP)||||Granite.|
24501|Squirrel Hills Granite|72682|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Doherty-Fig Tree Gully Domain area. Associated with Isan Orogeny (1590-1500 Ma).||Williams Supersuite|||Porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene-bearing granite and aplite.|
24501|Squirrel Hills Granite|72683|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Doherty-Fig Tree Domain area.   Associated with Isan Orogeny (1590-1500 Ma).||Williams Supersuite|||Porphyritic biotite and hornblende-biotite granite; minor equigranular granite, pyroxene-bearing granite and aplite.|
24501|Squirrel Hills Granite|72889|5|Briefly described|p8, p57.|||Provides a minimum age for the Hampden Slate.|1514+/-5 Ma, 1511+/-9 Ma.|||Intrudes Hampden Slate.||
35066|Squirrel Hills Suite|22515|4|Described|p403|||Comprises: Squirrel Hills, Mt Cobalt, Yellow Waterhole and Wimberu Granites.||||||
35066|Squirrel Hills Suite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.||Williams Supersuite.|Squirrel Hills Granite|||05-MAY-16
35066|Squirrel Hills Suite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite.|Includes Squirrel Hills Granite.|||
35066|Squirrel Hills Suite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Williams Supersuite|Includes Squirrel Hills Granite.|||
35066|Squirrel Hills Suite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Doherty-Fig Tree Gully Domain.||Williams Supersuite|Includes Squirrel Hills Granite.|||
35066|Squirrel Hills Suite|73553|6|Mentioned|p263|||||Wimberu Granite||||
29751|Staaten Metamorphic Group|23425|5|Briefly described|p371|||||||||
29751|Staaten Metamorphic Group|23430|5|Briefly described|p454|||Savannah Province.||||||
29751|Staaten Metamorphic Group|23496|5|Briefly described|Table 1||Proterozoic|~13km thick.||||||
29751|Staaten Metamorphic Group|43287|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29751|Staaten Metamorphic Group|43596|4|Described|Fig.6, p6,p15, p20 Tb. 1||Mesoproterozoic|Part of Savannah Province, together with Coen and Edward River Metamorphic Groups and the Holroyd Group. Does no outcrop.||||||27-JAN-09
29751|Staaten Metamorphic Group|43665|4|Described|p12-13||Proterozoic|||||||
29751|Staaten Metamorphic Group|43820|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29751|Staaten Metamorphic Group|69591|5|Briefly described|p76, p79|||Coen Inlier. Entirely concealed: based solely on geophysical interpretation. Forms a 170 x 70 km belt of prominent, subparallel elongate magnetic anomalies (prominent lows with minor highs). Total thickness is c.13 km. Planar nature suggests sediments and/or lavas.||||||
29751|Staaten Metamorphic Group|71792|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Savannah Province. This group is totally concealed by cover.||||||
29751|Staaten Metamorphic Group|73083|6|Mentioned|p76|||||||||
29214|Stanley Limestone Member|23032|5|Briefly described|p29 fig6|Devonian|Devonian|||||||
29214|Stanley Limestone Member|23424|5|Briefly described|Table 8.1||Middle Devonian|Age:  disparalis or, more probably asymmetricus Zone i.e. late Givetian or early Frasnian. Of Mytton Formation/Broken River Group, Graveyard Creek Subprovince.||||||
29214|Stanley Limestone Member|23431|5|Briefly described|p541|||Of Mytton Formation.||||||
29214|Stanley Limestone Member|23522|5|Briefly described|p250 Fig 6|Givetian|Givetian|||||||
29214|Stanley Limestone Member|24614|5|Briefly described|p202, p205|Frasnian|Givetian|Of the Mytton Formation. Highly fossiliferous, very shallow marine deposit. See also Stanley Member.||||||07-FEB-11
29214|Stanley Limestone Member|41260|3|Fully described|p70|||||||||
29214|Stanley Limestone Member|41679|2|Defined|p260|early Frasnian||||||||
29214|Stanley Limestone Member|41719|6|Mentioned|Fig.2|||||||||
29214|Stanley Limestone Member|41740|6|Mentioned|p222|||||||||
29214|Stanley Limestone Member|42031|5|Briefly described|Fig.5 p762|||||||||27-FEB-18
29214|Stanley Limestone Member|42032|6|Mentioned|Fig.12 P505|||||||||
29214|Stanley Limestone Member|42054|6|Mentioned|p273|||||||||
29214|Stanley Limestone Member|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
29214|Stanley Limestone Member|42933|3|Fully described|Table 2|||See also p124. Of Mytton Formation||||||
29214|Stanley Limestone Member|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
29214|Stanley Limestone Member|68336|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Mytton Formation.|||Bioclastic calcarenite, calcirudite and calcilutite; oolitic/oncolitic calcarenite to calcirudite; minor sandstone and siltstone.|
29214|Stanley Limestone Member|68341|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Mytton Formation.|||Bioclastic calcarenite, calcirudite and calcilutite; oolitic/oncolitic calcarenite to calcirudite; minor sandstone and siltstone.|
29214|Stanley Limestone Member|68478|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Mytton Formation.|||Bioclastic calcarenite, calcirudite and calcilutite; oolitic/oncolitic calcarenite to calcirudite; minor sandstone and siltstone.|
29214|Stanley Limestone Member|68479|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Mytton Formation.|||Bioclastic calcarenite, calcirudite and calcilutite; oolitic/oncolitic calcarenite to calcirudite; minor sandstone and siltstone.|
29214|Stanley Limestone Member|69592|5|Briefly described|p266-267, p298|Givetian|Givetian|Lang et al. (1989, 1993). Open, shallow, intertidal shelf deposits. Rare conodonts suggest it is no older than late Givetian.||Mytton Formation.|||A lower part of coarse- to very coarse-grained, planar to cross-bedded, ooid and oncolite grainstone and packstone, succeeded by thick-bedded bioclastic limestone (packstone to wackestone). Richly fossiliferous.|
36734|Stannary Hills Group|23423|6|Mentioned|p283|||Unsure if Stratigraphic unit or Mining Company.||||||
23989|Stannett Creek Gabbro|22847|3|Fully described|p 46|Devonian||||||||
23989|Stannett Creek Gabbro|23422|6|Mentioned|p175|||||||||
23989|Stannett Creek Gabbro|23513|5|Briefly described|Map legend|Silurian|Ordovician|Palaeozoic Intrusive No. 448.||||||
23989|Stannett Creek Gabbro|42054|6|Mentioned|p272|||||||||
23989|Stannett Creek Gabbro|42633|5|Briefly described|Table 1 P10|||||||||
23989|Stannett Creek Gabbro|42750|2|Defined|p40||Devonian|age of 407 +/- 5 Ma.||||||
23989|Stannett Creek Gabbro|43093|4|Described|Appendix 1||Devonian|||||||
23989|Stannett Creek Gabbro|43259|4|Described|Appendix 1,p48.|Early Devonian|Late Silurian|Rb-Sr age is 407+/-5 Ma. Also possible Ordovician - Early Silurian.||||||
23989|Stannett Creek Gabbro|43934|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
23989|Stannett Creek Gabbro|62075|6|Mentioned|p15 Fig.7|Early Devonian|Early Devonian|Appears as Stannett Creek gabbro.||||||
23989|Stannett Creek Gabbro|62521|5|Briefly described|p7 Tb. 1, p14|Devonian|Devonian|Age: 407+/-5Ma (Rb-Sr). Geological Province: Ravenswood Batholith. Comprises 3 or 4 contiguous plutons - containing two-pyroxene-olivine gabbros. Mafic intrusive rocks. May be Late Silurian to Early Devonian in age? See also p38-39, p44.||||||14-JAN-08
23989|Stannett Creek Gabbro|69592|6|Mentioned|p294|||Hutton and Crouch (1993). Shares some petrographic features with the Broughton River Granodiorite, suggesting they might be related.||||||
73988|Stanthorpe Supersuite|63748|5|Briefly described|p36-37|Early Triassic|Permian|Includes Stanthorpe and Bungulla Suites.||||||07-FEB-11
73988|Stanthorpe Supersuite|65455|6|Mentioned|p7|||New England Fold Belt. Has high U.||||||09-MAY-12
73988|Stanthorpe Supersuite|68111|5|Briefly described|p968 Tb.1|||Consistently mis-spelt as Stanthrope in Table 1. Also includes Dandahra Creek Leucogranite.|||Includes Mackenzie, Mount Mitchell, Sandy Flat, Undercliffe Falls, and Bungulla Monzogranites; Stanthorpe Granite; Nonnington, Mount Jonblee, Bolivia Range, and Billyrimba Leucomonzogranites;|||
73988|Stanthorpe Supersuite|68679|5|Briefly described|p454, p456-466|||Northern New England Batholith. Comprises a northern and southern part separated by Uralla and Hillgrove Supersuite granitoids. Geochemistry described. Associated with disseminated Au at Timbarra.|||Bungulla, Clare Hills, Herries, Sailor Jack, Stanthorpe, Ballandean, Mingimarny, Bullaganang, Mount You You, Suites.|||
73988|Stanthorpe Supersuite|69639|5|Briefly described|p1-p2, p9, p16, p20-p21, p26|Lopingian|Lopingian|New England Orogen. See also p50, p80, p157, p163, p175, p181-p182, p187, p218-p219, p221-p222.|||Includes the Stanthorpe Suite, Mount Mitchell Monzogranite, Bungulla Suite and the Bolivia Range Suite.|||
73988|Stanthorpe Supersuite|70217|5|Briefly described|v, vi, p60, p66, p74 tbl 14.1, p75, p76|Early Triassic|Late Permian|New England Orogen. Granites of this supersuite are I-type, felsic, fractionated and variably mineralised. Also includes the Billyrimba Leucomonzogranite, Ruby Creek Granite, Cullendore Granite, Stanthorpe Granite, Rivertree Granite, Bookookoorara Monzogranite, MacKenzie Monzogranite, Sandy Flat Monzogranite, Mount Mitchell Monzogranite, Mount Jonblee Leucomonzogranite and the Clive Monzogranite.  |255-238 Ma||Includes the Bolivia Range Suite, Morgans Creek Monzogranite.|||
73988|Stanthorpe Supersuite|70876|4|Described|p2, p58|Early Triassic|Early Triassic|New England Orogen. Donchak et al (2013) incorporated into this supersuite the Herries, Bullaganang, Ballandean and Mount You You supersuites despite their varied ages; the authors therefore suggest revisiting the defintion of this supersuite.|c. 248-245 Ma||Includes the Herries Suite.|||
73988|Stanthorpe Supersuite|71628|5|Briefly described|p5: 3, 6-7, 11; p7: 1-2; p9-1; p11: 1-3|Middle Triassic|Late Permian|See also p11: 5, 11, 25, 40; p12: 3, 9; p14: 2, 32; p15: 1-116; p16: 1-3, 10, 26; p18-10; p19: 37, 91, 131, 138, 144, 175. Redefined to exclude granites of the Cullendore Supersuite, and the Bungulla Type of Blevin and Chappell (1996). Previously included Bungulla Suite. The Supersuite is subdivided into several spatio-temporal groups (detailed). Geochemistry summarised; contrasted with Jibbinbar Leucosyenogranite.|256-241 Ma.||Stanthorpe Complex; Bolivia Range, Clive, Glen Eden, Surface Hill Suites.||Pale pink, mainly medium- to coarse-grained monzogranite-leucomonzogranite, in some cases transitional to syenogranite-leucosyenogranite. I-type.|
73988|Stanthorpe Supersuite|72528|5|Briefly described|p71, p109.|Triassic|Permian||c.254 to c.237 Ma||Includes Deepwater Syenogranite.|||
73988|Stanthorpe Supersuite|73570|6|Mentioned|p918|Middle Triassic|Middle Triassic|New England Orogen.||||||
77827|Stanwell Formation|68008|4|Described|p191, p231, p233, p243-244, p251|Early Cretaceous|Early Cretaceous|See also p254-255, p261-267. Name changed in this study (Murray et al., 2012). Previously the Stanwell Coal Measures, but only one occurrence of coal (Helby and Paltridge, 1977) has been found in the unit despite a century of exploration. Extends in an E-W belt, 15 x 3km, from Stanwell to Kalapa North. Crops out only along streams, esp. Neerkol Creek headwaters. 20-210m thick. Reported plant fossils are in fact from other units; an early Albian age is from palynological studies only. Age-equivalent to Burrum and Styx Coal Measures.||||Overlies Precipice Sandstone, and Dalma Basalt possibly conformably. Overlies, and is faulted against, Native Cat Andesite. At least partly correlated with Jim Crow beds.|A sequence of interbedded, finely laminated, fine-grained green to grey sandstone and dark grey carbonaceous siltstone, with sparse coaly laminae. Bioturbation is common throughout.|
77827|Stanwell Formation|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
77827|Stanwell Formation|68679|6|Mentioned|p312-313|Cretaceous|Cretaceous|Northern New England Orogen.||||||
77827|Stanwell Formation|69594|5|Briefly described|p551, p559-560|Albian|Albian|Murray (2007) and Murray et al. (2012). This name was applied to the lower (marginal marine) part of the Stanwell Coal Measures (Dunstan, 1898); the overlying part was assigned to the Razorback beds. Deltaic deposits.||||Overlies Precipice Sandstone, Mount Salmon Volcanics. Is overlain by Dalma Basalt.|Bioturbated and fossiliferous (microplankton-bearing) sandstone.|
80905|Starcke Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Starcke Suite.|||S-type granitoids.|
80906|Starcke Suite|60425|4|Described|p270-1 Appdx. 1|Late Permian|Late Permian|Of Cooktown Supersuite. Contains the informally named Starcke granite. S-type.||||||13-MAR-19
80906|Starcke Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Starcke Granite.||S-type granitoids.|
74793|Starcross Formation|67323|5|Briefly described|GIS attrib tbl, p19|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin.|1663 +/- 21 Ma (MDA: Carson et al., in prep.).|Kuridala Group.||Correlated with Llewellyn Creek Formation.|Psammite and pelitic schist containing garnet, staurolite and andalusite|
74793|Starcross Formation|67539|5|Briefly described|p13, p14|||Basal unit.||Of the Kuridala Group.||Equivalent of the  Llewellyn Creek Formation? Overlain by the New Hope Sandstone?||
74793|Starcross Formation|68146|4|Described|p3-4, p6, p112-120, p201, p211|||New name. Formerly mapped in part as the Kuridala Formation (now the Kuridala Group). Southern Kuridala-Selwyn zone, southern Marino-Stavely Domain. Age suggests this unit lies above the Gun Unconformity: age relationships with various units discussed. Has many similarities with Llewellyn Creek Formation but is significantly younger. Whole-rock Sm-Nd isotopic data tabulated.|1653 +/- 18 Ma maximum depositional age.|Basal Kuridala Group.||Tentatively correlated with Llewellyn Creek Formation.|A package of alternating muscovite(+/- andalusite) quartzo-feldspathic metapsammites, metapelites and sandstones.|
74793|Starcross Formation|69056|5|Briefly described|p55|||Maximum depositional age.|1663 +/- 21 Ma (Carson et al., 2011).|Basal Kuridala Group.||Is overlain by New Hope Sandstone.|Pelite/psammite-dominated.|
74793|Starcross Formation|69591|4|Described|p41, p43, p55|||Kuridala-Selwyn Domain, Calvert Superbasin. Part of Prize and Gun Supersequences. Submarine fan deposits. Another age given is 1673 +/- 9 Ma (Geoscience Australia, unpublished data); and on p55 the Carson et al. age is given as 1653 +/- 18 Ma.|1663 +/- 21 Ma (MDA:Carson et al., 2011).|Basal Kuridala Group.||Is overlain by New Hope Sandstone. Correlated with Llewellyn Formation.|Psammite and pelitic schist containing garnet, staurolite and andalusite.|
74793|Starcross Formation|69952|5|Briefly described|p4, p53|||Maximum depositional age. This conflicts with latest age determination for the Hampden Slate, suggesting the need to reassess current understanding of stratigraphic relationships in the Kuridala Group.|<1653 +/- 18 Ma (Carson et al., 2011).|Basal unit in Kuridala Group.||||
74793|Starcross Formation|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Basal Kuridala Group.||Overlies Roxmere Quartzite (Mount Albert Group). Is overlain by New Hope Sandstone.|Psammite and pelitic schist containing garnet, staurolite and andalusite.|05-MAY-16
74793|Starcross Formation|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala- Selwyn Domain. ||Kuridala Group.|||Psammite and pelitic schist containing garnet, staurolite and andalusite.|
74793|Starcross Formation|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.||Kuridala Group.|||Psammite and pelitic schist containing garnet, staurolite and andalusite.|20-JAN-22
74793|Starcross Formation|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Kuridala-Selwyn Domain.||Kuridala Group |||Psammite and pelitic schist containing garnet, staurolite and andalusite.|
74793|Starcross Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1653+/-18 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite.|
74793|Starcross Formation|72889|4|Described|p2-3, 5, 8, p32-36,p38-39,p43,p46-53.|Statherian|Statherian|Two sandstone samples provided maximum depositional ages. Previously mapped as part of the New Hope Sandstone, but now considered to be upper Starcross Formation.Previous maximum depositional age of Carson et al. 2011 also recalculated as 1694+/-11 Ma. These results support correlation with Soldiers Cap Group units. See also p54, p57. Refer to 1:250 000 sheet DUCHESS (SF5406). Age derived from Sensitive High Resolution Ion MicroProbe (SHRIMP) U-Pb zircon results.|1716 +/- 9 Ma, 1679 +/- 11 Ma max. dep ages.|Kuridala Group|Includes New Hope Sandstone Member|Conformably overlain by Hampden Slate. Correlative of Llewellyn Creek Formation and Mount Norna Quartzite.|Micaceous psammopelitic beds interbedded with coarse-grained, quartzose and locally feldspathic sandstone packages.|
23990|Starlight Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||01-JUN-09
23990|Starlight Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
23990|Starlight Granite|41235|6|Mentioned|Fig.2a|||||||||
23990|Starlight Granite|41740|6|Mentioned|p222|||||||||
23990|Starlight Granite|43259|6|Mentioned|Appendix 1,p34.||Carboniferous|Of Emuford/Emu Granite.||||||01-JUN-09
23990|Starlight Granite|60425|4|Described|p288-9 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, fine-grained to pegmatitic, slightly porphyritic to seriate, granophyric (topaz-fluorite-) biotite granite;  I-type. Included in Emuford Granite on most recent maps.||||||07-FEB-11
75654|Starvation Creek Complex|68679|5|Briefly described|p361, p365 Fig.5.52, p366 Fig.5.57|Permian|Permian|Northern Connors Subprovince. Early Permian. Foliated. REE plot.|291.6 +/- 1.8 Ma (U-Pb SHRIMP: Cross et al. 2012).||||Foliated biotite-hornblende granodiorite(?) with highly-attenuated mafic enclaves.|
75654|Starvation Creek Complex|68901|5|Briefly described|p4, p84-p86, p87, 88, 146|Permian|Permian|Northern New England Orogen, Bowen Region. Forms scattered outcrops in the bed of Starvation Creek. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.|291.6 +/- 1.8 Ma (SHRIMP U-Pb)||||Dated sample: White, medium-grained, uneven-grained to slightly porphyritic biotite-hornblende tonalite with sparse mafic inclusions and a well developed foliation.|15-NOV-18
75654|Starvation Creek Complex|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|292+/-1.8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite.|
75654|Starvation Creek Complex|73036|5|Briefly described|Map legend|Early Permian|Early Permian|Listed on the map as Subgroup rank.|||||Pale grey, fine to medium-grained, uneven-grained to slightly porphyritic biotite-hornblende tonalite to quartz monzodiorite or quartz diorite; with traces of titanite; extensively deformed and recrystallised.|
36397|Station Creek Igneous Complex|23608|4|Described|p49, p50 Fig 1 p52||Triassic|Previously Station Creek Adamellite. Previously mapped as a single magmatic unit and subsequently subdivided geochemically. Emplaced 250-220 Ma. I-type granites. North D'Aguilar Block.||||||
36397|Station Creek Igneous Complex|23609|4|Described|p11-12|||Constituent units renamed to reflect the rock type of the units. North D'Aguilar Block.||||||
36397|Station Creek Igneous Complex|68679|5|Briefly described|p409-411|Late Triassic|Late Triassic|Tang and Gust (2000). CONSTITUENTS (continued): One Mile Creek Granite; Yorkeys Diorite.|~237-210 Ma.||Station Creek, Woologa, Green Rock, Quartz Monzonites; Woonga Granodiorite; Mount Mucki Complex; Gibraltar Quartz Monzodiorite; Native Creek Microgranite; Black Snake Porphyry. See COMMENTS for more.||High-level I-type monzogabbro to monzogranite. Includes a high-K, calc-alkaline metaluminous group and a medium- to high-K, transitional calc-alkaline to tholeiitic metaluminous group. Variations occur from fractional crystallisation.|
26909|Station Mudstone Member|23037|6|Mentioned|p66||Permian|Of Barfield Formation.||||||
26909|Station Mudstone Member|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbrs].  Siltstone, mudstone.||||||
26909|Station Mudstone Member|30451|6|Mentioned|Fig.9|||See also P54||||||
26909|Station Mudstone Member|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
26909|Station Mudstone Member|41666|6|Mentioned|p3|||||||||
26909|Station Mudstone Member|43050|5|Briefly described|p52|||of Barfield Formation||||||
26909|Station Mudstone Member|44640|14|Not recorded|p32|||Member (basal) of Barfield Formation.||||||
26909|Station Mudstone Member|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Barfield Formation (Back Creek Group). Siltstone and mudstone.||||||18-JUN-09
26909|Station Mudstone Member|60330|5|Briefly described|p259|Late Permian|Late Permian|Of the Barfield Formation. Dark grey silty mudstone. Slightly fossiliferous, containing sponge spicules and foraminiferida. Geological Province: Bowen Basin.||||||
26909|Station Mudstone Member|65388|4|Described|p163 Fig. 63, p168, 169, 170|||Of Barfield Formation,  Bowen Basin. Redefined by Dear et al (1971) after Derrington & others (1959) formation. Type section along the Dawson Highway. Underlain by Cottenham Sandstone Member. Overlain by Flat Top Formation. May include tuffaceous rocks.||||||
30702|Steeles Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30702|Steeles Granite|50536|5|Briefly described|p1.5, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30702|Steeles Granite|67323|5|Briefly described|GIS attrib tbl, p12|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Exhibits NW trending linear fabric.||Sybella Suite|||Composite pluton containing a younger phase of porphyritic biotite granite intruding an older strongly foliated and gneissic granodiorite to diorite phase.|
30702|Steeles Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Composite pluton containing a younger phase of porphyritic biotite granite intruding an older strongly foliated and gneissic granodiorite to diorite phase.|
75140|Stingaree granite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name. Of the Bedarra Suite (Bedarra Batholith or Supersuite?) in the Bedarra Granite Belt. White, medium- to coarse-grained biotite granite. I-type.||||||07-FEB-11
36258|Stingo Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36258|Stingo Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
36258|Stingo Granite|60425|4|Described|p285 Appdx., p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Included in Black Prince Granite, together with Brownville, Disaster, Glenlinedale and Wilderness Granites on most recent maps.Fine-grained, porphyritic biotite granite. I-type.||||||07-FEB-11
36266|Stinking Cornishman Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36266|Stinking Cornishman Microgranite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36266|Stinking Cornishman Microgranite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Topaz-bearing microgranite; I-type. Included in Wild Granite on most recent maps.||||||07-FEB-11
29333|Stirlington Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Ootann Suite. Intrudes Dargalong Metamorphics, Ootann Granite. Age:  301-302Ma. Geological Province: Georgetown Region.||||||30-MAR-15
29333|Stirlington Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
29333|Stirlington Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~301-302 Ma, Rb-Sr. of Ootann Supersuite.||||||
29333|Stirlington Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 319. I-Type.||||||
29333|Stirlington Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
29333|Stirlington Granite|43083|5|Briefly described|p256|||Of Ootann Supersuite. Intrudes Ootann Granite and dargalong Metamorphics. I-type.  Lithology included.||||||17-JUN-09
29333|Stirlington Granite|43087|2|Defined|p46|Late Carboniferous||Rb-Sr age 301-302 Ma. Of Ootann Supersuite. Reserved as Stirlington.||||||
29333|Stirlington Granite|43259|4|Described|Appendix 1,p38.||Late Carboniferous|Age is 302 Ma.||||||
29333|Stirlington Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Age: 302-301Ma (Rb-Sr). I-type. Pink, med.-grained, even-grained hornblende-biotite granite; inclusions rare; allanite a prominent accessory locally.||||||07-FEB-11
29333|Stirlington Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pink, medium-grained, even-grained, leucocratic hornblende-biotite granite; with accessory allanite and rare enclaves.|
22897|Stones Creek Volcanics|22675|2|Defined|p24|Early Carboniferous|Devonian|Drummond Basin||||||
22897|Stones Creek Volcanics|23504|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
22897|Stones Creek Volcanics|23513|5|Briefly described|Map legend|Carboniferous|Devonian|Palaeozoic Volcanic No. V71. I-Type.||||||
22897|Stones Creek Volcanics|43259|4|Described|Appendix 1,p7.|Early Carboniferous|Late Devonian|U-Pb zircon dated at 365+/-5Ma.||||||
22897|Stones Creek Volcanics|43391|5|Briefly described|Map legend|Late Devonian|Late Devonian|Geological Province: Drummond Basin. Late Devonian and/or Early Carboniferous.  Dacitic ignimbrite.||||||23-JUN-04
22897|Stones Creek Volcanics|43727|6|Mentioned|p1|||||||||
22897|Stones Creek Volcanics|43734|5|Briefly described|p10|||||||||
22897|Stones Creek Volcanics|43936|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
22897|Stones Creek Volcanics|60659|4|Described|p13|Late Devonian|Late Devonian|Rhyolitic ignimbrite + lava, sandstone + volcaniclastic sandstone, andesitic lava + well-bedded fragmental dacitic to andesitic rocks. Overlies Saint Anns Fm; underlie Scartwater Formation. Age: ~357Ma. Geol Prov: Drummond Basin.||||||07-FEB-11
22897|Stones Creek Volcanics|64852|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Volcaniclastic siltstone and sandstone; andesitic breccia; dacitic ignimbrite and lava; intrusive rhyolite.||||||
22897|Stones Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Bimurra, Foyle and Silver Hills Volcanics, and the Mount Wyatt and Saint Anns Formations, are all mapped under the symbol, DCD1.||||||
22897|Stones Creek Volcanics|68679|6|Mentioned|p364|Early Carboniferous|Late Devonian|Thomson Orogen.||||||
22897|Stones Creek Volcanics|68731|6|Mentioned|p193|||Oversby et al. (1994). See also Stone Creek Volcanics.|||||Silicic to intermediate ignimbrite and lava with subordinate volcanilithics including pebble to cobble conglomerate, sandstone and siltstone.|18-JUL-14
22897|Stones Creek Volcanics|68900|3|Fully described|p4, p37-p38, p44-p47, p52, p62|Early Carboniferous|Late Devonian|Drummond Basin. Originally described by Olgers (1972) who considered it equivalent to the Mount Wyatt Formation. Named the Stones Creek Volcanics by Oversby et al (1994). Crops out in the north-eastern part of HARVEST HOME producing hilly topography. Outcrops more extensively in GLENDON. These rocks have a moderately high response on airborne magnetic images and have a moderately high potassium signature on airborne radiometrics. Strongly welded ignimbrites suggest a subaerial depositional environment. Olgers estimated thickness to be roughly 450m. Fossil assemblage is provided. Possibly equivalent to the Vera-Nancy Volcanics and potential age equivalent to the Silver Hills Volcanics.||||(probably) overlies the Mount Windsor Volcanics. Overlain by the Scartwater Formation (conformably or disconformably).|Lithic-poor, purple to brown ignimbrite containing sparse clasts of felsic volcanics and siltstone.Rhyolitic lavas, andesitic lavas, dacitic lavas and volcanolithic sedimentary rocks including pebble to cobble conglomerate.|
22897|Stones Creek Volcanics|68901|6|Mentioned|p2 Fig. i|Early Carboniferous|Late Devonian|Drummond Basin.||||||27-SEP-18
22897|Stones Creek Volcanics|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|Thomson Orogen.||||||
22897|Stones Creek Volcanics|70740|4|Described|i, iii, p2, p8, p9|Carboniferous|Devonian|Drummond Basin. Previously mapped and recognised by Olgers 1972 but unnamed; during this period the lower part of the unit was correlated with the Mount Wyatt Formation and lower Saint Anns Formation whilst the upper part was considered equivalent of the Saint Anns Formation or Silver Hills Volcanics. Some rocks previously mapped as this unit have been reassigned to the Star of Hope Formation. Inherited zircon SHRIMP ages given on p8 from Black 1994, however for this unit SHRIMP ages are scarce and considered unreliable, thus age is based primarily on fossil assemblage. Distribution and fossil assemblage are discussed. Up to 3000m thick sequences described by Oversby et al., 1994. [NB the author states that there is some uncertainty regarding the stratigraphic position and age of this unit]. Overlain by the Mount Hall Formation, Star of Hope Formation and the Bulgonunna Volcanics. Equivalent to the Bimurra Volcanics, Saint Anns Formation and the Silver Hills Volcanics. See also p41-p42, p76-p80, p84, p88, p106, p123.||||Unconformably overlies the Mount Windsor Volcanics. Conformably overlain by the Scartwater Formation.|Porphyritic andesite or dacite lavas interbedded with pyroclastic or epiclastic deposits. Interbedded clastic deposits of dacitic breccia/ignimbrite, bedded quartz-feldspar, lithic arenite, siltstone and rarely mudstone also occur.|
22897|Stones Creek Volcanics|71592|5|Briefly described|Appendix A.|||Drummond Basin.|357+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Andesite.|
38237|Stonington Granite|23422|5|Briefly described|p212 Table 6.7|||||||||
41937|Stony Creek Granite|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Pale pink to white, fine to medium grained, even grained to highly porphyritic hornblende biotite and (muscovite) biotite monzogranite.||||||21-OCT-04
41937|Stony Creek Granite|60473|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Pale pink to white, fine to medium grained, even-grained to highly porphyritic hornblende-biotite and (muscovite-) biotite monzogranite.||||||21-OCT-04
41937|Stony Creek Granite|63612|6|Mentioned|p17, p25|||Referred to as the 'Stony Creek Granite body' - not intended as a formal name. Displays a strong magnetic anomaly on eastern margin.||||||07-FEB-11
41937|Stony Creek Granite|65388|2|Defined|p382-383, p135 Fig. 53, p362, 397|Early Permian|Late Carboniferous|Northern Connors Arch. Most relationships uncertain. Interpreted to post-date Strathdee Granodiorite. Tentative age given.  Heterogeneity and complex relationships imply this is a multiphase pluton. Fine-grained (average grainsize of groundmass grains ~0.3mm), moderately porphyritic, leucocratic hornblende-biotite monzogranite at type locality.||||||
29023|Stopem Blockem Conglomerate Member|23032|5|Briefly described|p31||Early Devonian|||||||
29023|Stopem Blockem Conglomerate Member|23291|5|Briefly described|p37|Carboniferous|Late Devonian|Parent: Bulgeri Formation. Geological Province: Georgetown Region.||||||08-JUL-15
29023|Stopem Blockem Conglomerate Member|23424|5|Briefly described|Table 8.1 p336.||Late Devonian| Of Bulgeri Formation/Bundock Creek Group, Bundock Basin.||||||
29023|Stopem Blockem Conglomerate Member|23430|5|Briefly described|p508|||Of Bulgeri Formation. Bundock Basin Province.||||||
29023|Stopem Blockem Conglomerate Member|41260|3|Fully described|p85|||Reserved as Stopem Blockem Formation.||||||
29023|Stopem Blockem Conglomerate Member|41675|6|Mentioned|p71|||||||||
29023|Stopem Blockem Conglomerate Member|41679|6|Mentioned|Fig.2|||||||||
29023|Stopem Blockem Conglomerate Member|41719|6|Mentioned|Fig.2|||||||||
29023|Stopem Blockem Conglomerate Member|41739|2|Defined|p301|Famennian|Frasnian|||||||
29023|Stopem Blockem Conglomerate Member|41740|6|Mentioned|p222|||||||||
29023|Stopem Blockem Conglomerate Member|42054|6|Mentioned|p273|||||||||
29023|Stopem Blockem Conglomerate Member|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
29023|Stopem Blockem Conglomerate Member|42709|6|Mentioned|map legend|||||||||
29023|Stopem Blockem Conglomerate Member|42933|4|Described|p130|||of Bulgeri Formation||||||
29023|Stopem Blockem Conglomerate Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bulgeri Formation.||||||
29023|Stopem Blockem Conglomerate Member|68336|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.||Overlies Rockfields Member.|Red, coarse-grained lithic sandstone and polymictic conglomerate; minor fine-grained redbeds and calcirudite (reworked from the Waldo Vale Subgroup).|
29023|Stopem Blockem Conglomerate Member|68341|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.||Overlies Rockfields Member.|Red, coarse-grained lithic sandstone and polymictic conglomerate; minor fine-grained redbeds and calcirudite (reworked from the Waldo Vale Subgroup).|
29023|Stopem Blockem Conglomerate Member|68478|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin. Shown as older than the Jamieson Member and younger than the Rockfields Member.||Of the Bulgeri Formation.|||Red, coarse-grained lithic sandstone and polymictic conglomerate; minor fine-grained redbeds and calcirudite (reworked from the Wando Vale Subgroup).|
29023|Stopem Blockem Conglomerate Member|68479|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Of the Bulgeri Formation.||Shown as older than the Jamieson Member and younger than the Rockfields Member.|Red, coarse-grained lithic sandstone and polymictic conglomerate; minor fine-grained redbeds and calcirudite (reworked from the Wando Vale Subgroup).|
29023|Stopem Blockem Conglomerate Member|69030|5|Briefly described|p6|Devonian|Devonian|Bundock Basin (Broken River Province).||Bulgeri Formation.||||
29023|Stopem Blockem Conglomerate Member|69592|4|Described|p259, p273-274, p276, p298|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. Widespread unit, up to 270m thick. Forms prominent ridges. Clasts sourced from western parts of the Camel Creek Subprovince.|~374 Ma.|Bulgeri Formation.||Overlies Rockfields Member. Is overlain by Jamieson Member.|Medium- to thick-bedded, coarse to very coarse, pebbly lithic sandstone, and red pebble to cobble conglomerate with local small boulders.|
82793|Storm King Monzogranite|71628|5|Briefly described|p12: 1, 9-10, 15-17; p15: 33, 52|||New name. Primarily occurs along E reaches of Storm King Dam, from which it is named. Forms a 5 x 3 km, deeply weathered and poorly exposed pluton 8 km SE of Stanthorpe. Limited geochemistry described; similar to Gleamwoods Monzogranite.||Gleamwoods Suite.||Is entirely enclosed by the younger Jenners Monzogranite (Stanthorpe Complex).|Pale grey, medium-grained, coarsely porphyritic hornblende-biotite monzogranite; locally flow-aligned. I-type.|
82148|Strathbogie Trachyte|73029|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Flow-banded trachyte lava, volcaniclastics and/or intrusives.|
28096|Strathburn Formation|22781|4|Described|p22|Proterozoic|Proterozoic|Holroyd Group||||||
28096|Strathburn Formation|23420|5|Briefly described|p 143 table 4.4 + p 120|||In the Holroyd Group. Thickness 1000m||||||
28096|Strathburn Formation|23431|5|Briefly described|p535|||of Holroyd Group.||||||
28096|Strathburn Formation|43596|4|Described|p19 Tb. 1, p23|Mesoproterozoic|Mesoproterozoic|Of Holroyd Gp. Biotite-muscovite-qtz schist with, variously, graphite, sillimanite, garnet, andalusite+tourmaline; quartzite; mica-feldspar gneiss. More extensive on EBAGOOLA where it is typically med.-coarse-gr., deeply weathered muscovite-quartz schist.||||||05-NOV-08
28096|Strathburn Formation|43738|6|Mentioned|p48|||||||||
28096|Strathburn Formation|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group||||||24-JAN-05
28096|Strathburn Formation|63866|5|Briefly described|p80|Calymmian|Calymmian|Savannah Province, Coen Region.|1430 +/- 10 Ma (Black, OZCHRON)|Holroyd Group||||
28096|Strathburn Formation|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. Extensive unit along eastern margin. 1000m thick; top not exposed.||Holroyd Group.|||Mudstone, siltstone, slate, phyllite, graphite-mica schist, muscovite-biotite gneiss, quartzite.|
28096|Strathburn Formation|71592|5|Briefly described|Appendix A.|||Savannah Province.|1430+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
28096|Strathburn Formation|71849|6|Mentioned|p8, p195|Mesoproterozoic|Mesoproterozoic|||Holroyd Group.||||
28096|Strathburn Formation|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|Four facies variations (lithologies described in map legend) are mapped separately.||Holroyd Group.||Partly interlayered with Strathburn Formation.|Muscovite-biotite-quartz gneiss, sillimanite-mica-quartz schist; andalusite, graphite, staurolite, garnet, chloritoid and rare kyanite in places; some quartzite.|
28096|Strathburn Formation|73387|6|Mentioned|p37|||Black (1996) reported an age of 1430 +/- 10 Ma from zircon rims.||Holroyd Group||||19-DEC-22
78957|Strathdee Granodiorite|65388|2|Defined|p383-384, 135, 362, 363, 364, 365, 375|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Intrudes Leura Volcanics. Interpreted to intrude Mount Maryvale Granodiorite. Intruded by Whitehorse Granite. Interpreted to pre-date Stony Creek Granite and Featherstone, Carminya and Epsom Granodiorites. Tentative age given. Mainly grey or brown to dark reddish brown (weathered), fine to medium-grained, uneven-grained to slightly porphyritic hornblende-biotite granodiorite and biotite-hornblende granodiorite. See also p382, 397.||||||
29753|Strathleven Granite|43596|4|Described|p34, p28 Tb. 3|||Uassigned S-type granite. Intrudes Yambo metamorphic Group and may(?) intrude Aralba Granite also. Pale brown to grey, moderately porphyritic biotite-muscovite granite with K-fledspar and muscovite phenocrysts.||||||27-NOV-19
29753|Strathleven Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
28104|Strathmay Formation|22781|4|Described|p24|Proterozoic|Proterozoic|Holroyd Group||||||
28104|Strathmay Formation|23420|5|Briefly described|p 143 table 4.4 + p 120|||In the Holroyd Group.||||||
28104|Strathmay Formation|43738|6|Mentioned|p48|||||||||
28104|Strathmay Formation|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. Crops out between Lukin and Holroyd Rivers. Top not exposed.||Holroyd Group.|||Slate and biotite to garnet-biotite schist.|
28104|Strathmay Formation|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Holroyd Group.|||Brown to purple garnet-biotite schist with rare sillimanite and andalusite, and thin-bedded quartzite in lower part; grey slate and biotite phyllite in upper part.|
31112|Strathtay Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31112|Strathtay Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
31112|Strathtay Granodiorite|43480|2|Defined|7-31|Devonian|Silurian|||||||
31112|Strathtay Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.|410 +/- 6 Ma (SHRIMP U-Pb zircon).|Upland Supersuite.|||I-type.|
29628|Strophalosia clarkei Bed|42994|6|Mentioned|p275|||||||||
30453|Stuart Pocket Granite|22675|4|Described|p96|Paleozoic|Paleozoic|||||||07-NOV-08
30453|Stuart Pocket Granite|23504|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30453|Stuart Pocket Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 219. I-Type.||||||
30453|Stuart Pocket Granite|43259|5|Briefly described|Appendix 1,p31|Permian|Carboniferous|||||||
30453|Stuart Pocket Granite|43391|5|Briefly described|Map legend|Permian|Carboniferous|Carboniferous and/or Permian.  Coarse biotite granite.||||||23-JUN-04
30453|Stuart Pocket Granite|43936|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
30453|Stuart Pocket Granite|70740|5|Briefly described|p78, p129|||Outcrop characteristics and distribution briefly discussed.|||||Deformed, coarse-grained biotite granite.|
33432|Stuart River Granite|23799|3|Fully described|p72, p19|Triassic|Permian|See also p13 Tb. 1.  Formerly included as part of  Boondooma Complex.  Age: 255.5+/-5.6Ma to 250+/-0.8Ma (Ar/Ar - Vasconcelos and Feng, 2000). Intrudes Fifer Creek Metamorphics.  Of the South-east Qld. Volcanic and Plutonic Intrusives.||||||
33432|Stuart River Granite|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
33432|Stuart River Granite|60371|5|Briefly described|Map Legend|Triassic|Permian|Even-grained biotite leucogranite.||||||
33432|Stuart River Granite|68679|5|Briefly described|p323, p414-415|Early Triassic|Permian|West of the Esk Basin, northern New England Orogen. Proximity to this unit (and other named units) increases the metamorphic grade of rocks in the Fifer Creek Metamorphics. Has lower Na2O and K2O and higher CaO. Both Ar-Ar (biotite) age determinations by Cranfield et al. (2001).|255.5 +/- 0.6 Ma and 250.0 +/- 0.8 Ma.||||Cream, fine- to medium-grained (rarely coarse), equigranular leucocratic granite, networks of anastomosing mylonitic shears and brittle fractures most intense in the south; relatively homogeneous granite with penetrative foliation.|
22912|Stuarts Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Wakara Volcanic Subgroup of Featherbed Volcanic Group.||||||
22912|Stuarts Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V104. A-Type.||||||
22912|Stuarts Rhyolite|23616|6|Mentioned|Table 3 p47|||||||||
22912|Stuarts Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
22912|Stuarts Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Wakara Volcanic Subgroup.||||||
22912|Stuarts Rhyolite|43259|4|Described|Appendix 1,p10.||Early Permian|of Wakara Volcanic Subgroup.||||||
22912|Stuarts Rhyolite|43626|2|Defined|p75||Early Permian|Age between 289+/-10 Ma and 278+/-3 Ma||||||
22912|Stuarts Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
22912|Stuarts Rhyolite|60425|5|Briefly described|p44 Tb. 3|Early Permian|Early Permian|Informal subunit of Wakara Volcanic Subgroup (Fatherbed Volcanic Group).||||||07-FEB-11
22914|Subkin Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 302. I-Type.||||||
22914|Subkin Granodiorite|23713|5|Briefly described|p74 Appendix 2|||Intrudes Kitoba Member of the Hodgkinson Formation.||||||
22914|Subkin Granodiorite|43083|4|Described|p253|||Of the Almaden Supersuite. I-type.  Lithology included.||||||17-JUN-09
22914|Subkin Granodiorite|43254|5|Briefly described|map legend||Late Carboniferous|of Almaden Supersuite.||||||
22914|Subkin Granodiorite|43259|4|Described|Appendix 1,p37.||Late Carboniferous|||||||
22914|Subkin Granodiorite|43625|6|Mentioned|p49|||||||||
22914|Subkin Granodiorite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Grey, fine-grained, modersately to highly porphyritic (hornblende-) biotite granodiorite; mafic enclaves to 1m common. I-type.||||||07-FEB-11
23996|Sues Creek Microgranite|23032|4|Described|p45||Early Carboniferous|||||||
23996|Sues Creek Microgranite|23291|4|Described|p50, p98 Tb. 3.11|Carboniferous|Carboniferous|Intrudes the Butlers Volcanic Group. Geological Province: Georgetown Region.||||||28-MAY-15
23996|Sues Creek Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 32. I-Type.||||||
23996|Sues Creek Microgranite|23619|4|Described|p40 Table 2||Carboniferous|Intrudes Einasleigh Metamorphics, Oak River Granodiorite and Butlers Volcanic Group.||||||
23996|Sues Creek Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
23996|Sues Creek Microgranite|40542|6|Mentioned|p97|||||||||
23996|Sues Creek Microgranite|43113|4|Described|Table 2 p25||Carboniferous|||||||
23996|Sues Creek Microgranite|43253|5|Briefly described|map legend||Carboniferous|||||||
23996|Sues Creek Microgranite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
23996|Sues Creek Microgranite|43286|5|Briefly described|Map Legend||Carboniferous|||||||
23996|Sues Creek Microgranite|43664|6|Mentioned|p96|||||||||
23996|Sues Creek Microgranite|43740|4|Described|p29||Carboniferous|||||||
23996|Sues Creek Microgranite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
23996|Sues Creek Microgranite|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23996|Sues Creek Microgranite|50201|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
23996|Sues Creek Microgranite|50211|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Pink porphyritic hornblende-biotite and biotite microgranite.||||||14-MAY-04
23996|Sues Creek Microgranite|68346|5|Briefly described|Map legend.|Carboniferous|Carboniferous|The legend gives these lithologies for this unit: microdiorite, dolerite, gabbro and intrusive andesite: none of which fits a 'microgranite'. It seems most likely that this description has been erroneously swapped with that of an un-named unit coded Cia, whose lithologies are : pink porphyritic hornblende-biotite and biotite microgranite, a description of Sues Creek Microgranite already in the database from another article. Unit in Lochaber Ring Structure.||||||
23996|Sues Creek Microgranite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Pink porphyritic hornblende-biotite and biotite microgranite.|
23996|Sues Creek Microgranite|68357|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Lochaber Ring Structure, Kennedy Province.|||||Pink porphyritic hornblende-biotite and biotite microgranite.|
23996|Sues Creek Microgranite|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Lochaber Ring Structure.|||||Pink porphyritic hornblende-biotite and biotite microgranite.|
23996|Sues Creek Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Glenmore Batholith. Unassigned.|||||Hornblende-biotite microgranite. I-type.|
23997|Sugar Bag Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
23997|Sugar Bag Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 267. I-Type.||||||
23997|Sugar Bag Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
23997|Sugar Bag Granite|41235|6|Mentioned|Fig.2a|||||||||
23997|Sugar Bag Granite|41740|6|Mentioned|p222|||||||||
23997|Sugar Bag Granite|43259|4|Described|Appendix 1,p35.||Carboniferous|||||||
23997|Sugar Bag Granite|60425|4|Described|p288-9 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink to cream, medium-grained, poprhyritic (topaz-) biotite granite;  I-type. Includes Bloodwood Granite on most recent maps.||||||07-FEB-11
29759|Sugarbag Creek Quartzite|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
29759|Sugarbag Creek Quartzite|22781|4|Described|p18|Proterozoic|Proterozoic|Holroyd Group||||||13-JAN-05
29759|Sugarbag Creek Quartzite|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group. Correlates with Drovers Lagoon Formation. Thickness 1200m||||||
29759|Sugarbag Creek Quartzite|24089|5|Briefly described|Student Activites|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group.||||||
29759|Sugarbag Creek Quartzite|43596|4|Described|p18p19 Tb. 1||Proterozoic|Of the Holroyd Group. Conformably overlies Dinah Formation. Max. thickness: 1200m. Comprises 4 variants or subunits based on metamorphic grade for which detailed lithology is provided.||||||27-JAN-09
29759|Sugarbag Creek Quartzite|43820|5|Briefly described|Map Legend||Mesoproterozoic|Holroyd Group||||||24-JAN-05
29759|Sugarbag Creek Quartzite|69591|5|Briefly described|p79 Tb.2.6|||Savannah Province, Coen Inlier. 1200m thick. Forms elongate, folded and faulted bands south of Edward River.||Holroyd Group.||Correlates with Drovers Lagoon Formation.|Quartzite, slate, phyllite, schist, some gneiss. More pelitic to the south.|
41257|Sujeewong Gabbro|50598|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Layered medium to coarse grained hornblende gabbro and quartz gabbro.||||||
41257|Sujeewong Gabbro|65388|2|Defined|p276, p236 Fig. 81|Late Carboniferous|Late Carboniferous|Previously included in Kilbeggan Adamellite by Whitaker & others (1974). Probably intrudes the Ah Fat Granodiorite Complex and Glisson Granodiorite. K-Ar dating of hornblende gave a (recalculated) late Carboniferous age of 310+/- 9Ma (Green, 1975 and other refs). Renaming to Sujeewong Diorite considered, but not used herein. Dark grey to black, medium to coarse-grained clinopyroxene-biotite-hornblende diorite or gabbro.||||||
41257|Sujeewong Gabbro|68679|5|Briefly described|p406, p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.|310 +/- 9 Ma (K-Ar hbl: Whitaker et al. 1974).|||Probably intrudes Ah Fat Granodiorite Complex and Glissons Granodiorite.|Grey to black, medium- to coarse-grained clinopyroxene-biotite-hornblende diorite or gabbro.|
24510|Sulieman Gneiss|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Yaringa Metamorphics. Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
24510|Sulieman Gneiss|24419|5|Briefly described|p14, p12 Fig. 4, p15 Fig. 6|Proterozoic|Proterozoic|Intruded by Sybella Suite granites.  Highly deformed and metamorphosed volcanics and sediments.  Unconformably overlain by Jayah Creek and Oroopo Metabasalts. Geol.Prov: Western Fold Belt, Leichardt River Subprovince (Mount Isa Orogen)||||||13-APR-05
24510|Sulieman Gneiss|37862|4|Described|p586|||||||||
24510|Sulieman Gneiss|38234|4|Described|p103|||||||||
24510|Sulieman Gneiss|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24510|Sulieman Gneiss|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24510|Sulieman Gneiss|38658|6|Mentioned|p153|||||||||
24510|Sulieman Gneiss|39445|5|Briefly described|Table 2|||||||||
24510|Sulieman Gneiss|40840|6|Mentioned|Map legend|||||||||
24510|Sulieman Gneiss|41381|6|Mentioned|p325|||||||||
24510|Sulieman Gneiss|41978|4|Described|p498|||||||||
24510|Sulieman Gneiss|41979|6|Mentioned|Fig.2 P512|||||||||
24510|Sulieman Gneiss|45161|4|Described|p10|||||||||
24510|Sulieman Gneiss|45166|6|Mentioned|p7|||||||||
24510|Sulieman Gneiss|49009|2|Defined|p46|Precambrian|Precambrian|Previously mapped as part of E.Creek Volc. & Sybella Gr.(Noakes etc.59).||||||
24510|Sulieman Gneiss|49041|5|Briefly described|Table 1|||||||||
24510|Sulieman Gneiss|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
24510|Sulieman Gneiss|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Gneiss, amphibolite, quartzite.||||||
24510|Sulieman Gneiss|60513|6|Mentioned|p283, p281 fig 2, p287 fig 3, p288|||||||||
24510|Sulieman Gneiss|61933|5|Briefly described|p169 Fig.1|||||||||
24510|Sulieman Gneiss|63866|5|Briefly described|p57|Orosirian||Leichhardt River Fault Trough.|>1850 Ma|||||
24510|Sulieman Gneiss|64250|6|Mentioned|p9 fig 1, p11 fig.3, p19|||Basement of Western Fold Belt, Mount Isa Inlier.||||||
24510|Sulieman Gneiss|64254|5|Briefly described|p160 Fig. 1, p165|||Geological Province: Kalkadoon - Leichhardt Belt.||||||
24510|Sulieman Gneiss|65396|6|Mentioned|p82, p172, p175, p186, p241, p438 Fig.1|||Basement to Kalkadoon-Leichhardt Belt, Lawn Hill Platform.||||||
24510|Sulieman Gneiss|67323|5|Briefly described|GIS attrib tbl, p29, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Sybella Domain. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny.|||||Felsic gneiss, augen gneiss, hornblende schist, amphibolite, quartzite.|
24510|Sulieman Gneiss|68553|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Pre-Barramundi Orogeny basement. This unit, as well as Saint Ronans and Yaringa Metamorphics, are all mapped under the symbol, -Px.||||||
24510|Sulieman Gneiss|69591|5|Briefly described|p29-31, p58|Paleoproterozoic|Paleoproterozoic|One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma).|||||Quartzofeldspathic gneiss, augen gneiss, hornblende schist, amphibolite, calc-silicate and quartzite.|
24510|Sulieman Gneiss|72889|6|Mentioned|p6 Fig.i.|||||||||
24510|Sulieman Gneiss|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Metamorphics.|
75611|Summer Hill Gabbro|69594|5|Briefly described|p567|Cretaceous|Cretaceous|Bowen-Mackay region. A determination of 116.7 +/- 12.2 Ma (K-Ar biotite: Allen et al., 1998) may be a reset age.|135.2 +/- 2.8 Ma (K-Ar hbl: Allen et al. 1998).|||||
75611|Summer Hill Gabbro|73029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Age shown as uncertain.|||||Dark grey to dark greenish-grey, fine to medium-grained, uneven-grained gabbro, norite and subordinate anorthosite, diorite, quartz diorite; minor chromitite.|
30889|Sunbeam Granodiorite|22675|4|Described|p98|Carboniferous|Carboniferous|||||||
30889|Sunbeam Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 240. I-Type.||||||
30889|Sunbeam Granodiorite|43391|5|Briefly described|Map legend|Permian|Carboniferous|Carboniferous and/or Permian.  Melanocratic fine to medium granite to granodiorite.||||||23-JUN-04
30889|Sunbeam Granodiorite|68900|6|Mentioned|p26, p30|||||||Intrudes the Ukalunda Formation.||
30889|Sunbeam Granodiorite|70740|5|Briefly described|p28, p34, p49, p105, p129|Permian|Carboniferous|Outcrop characteristics briefly discussed.||||Intrudes the Ukalunda Formation, Les Jumelles Beds, Mount Wyatt Formation. Faulted against the Joe-de-Little Granodiorite and the Hidden Valley Rhyolite.|Melanocratic, fine to medium-grained hornblende-biotite granite to granodiorite.|
34668|Sunburst Suite|22847|6|Mentioned|p 10|||||||||
34668|Sunburst Suite|23422|4|Described|p173, p210 Table 6.6|Early Ordovician|Early Ordovician|Intrudes Charters Towers Metamorphics.||||||
34668|Sunburst Suite|23893|5|Briefly described|p13|Early Ordovician|Late Cambrian|||||||
34668|Sunburst Suite|62521|5|Briefly described|p30|Early Ordovician|Late Cambrian|Includes Sunburst Granodiorite. Geological Province: Ravenswood Batholith. See al;so p1, p26.||||||14-JAN-08
34668|Sunburst Suite|68553|6|Mentioned|Map legend|Ordovician|Ordovician|Charters Towers Province. This unit, as well as the Brittany, Chipley, Columbia Creek (part), Hogsflesh and Lavery Creek Supersuites; the Schreibers Suite; the Lynwater Complex; and various ungrouped plutonic units, are all mapped under the same symbol, Ogm.||||||
34668|Sunburst Suite|68731|6|Mentioned|p151 Fig 3.51|Ordovician|Ordovician|||||||
80779|Sundown Creek Diorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, fine-grained hornblende-clinopyroxene diorite; deeply weathered and poorly exposed.|
36233|Sundown Granite|23291|5|Briefly described|p101 Tb. 3.12|Late Carboniferous|Late Carboniferous|Of the O'Brien's Creek Supersuite. Intruded by Sandy Tate Granite, Rudd Granite (Ootann Supersuite). Geological Province: Georgetown Region.||||||01-JUL-15
36233|Sundown Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||18-JAN-07
36233|Sundown Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 359. I-Type.||||||
36233|Sundown Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of the O'Briens Creek Supersuite.||||||18-JAN-07
36233|Sundown Granite|23624|4|Described|p20|||Of the O'Brien's [misspelling of O'Briens] Creek Supersuite.||||||08-JUL-15
36233|Sundown Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink to cream, medium- to coarse-grained granite; commonly altered.|
36233|Sundown Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pink to cream, medium- to coarse-grained granite; commonly altered.|
36234|Sundown Volcanic Group|23291|4|Described|p38, p92 Tb. 3.9|Late Carboniferous|Late Carboniferous|Geological Province: Georgetown Region.||||||08-JUL-15
36234|Sundown Volcanic Group|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
36234|Sundown Volcanic Group|23616|5|Briefly described|Table 3 p54|||Dargalong Province.||||||
36234|Sundown Volcanic Group|23624|4|Described|p21|||||||||
36234|Sundown Volcanic Group|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Gingerella and Kallon Cauldron Complexes.|||
36234|Sundown Volcanic Group|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.|||Includes Gingerella and Kallon Cauldron Complexes.|||
36234|Sundown Volcanic Group|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province|||Includes Gingerella Volcanics.|||
36234|Sundown Volcanic Group|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range and Maureen Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
36234|Sundown Volcanic Group|69593|6|Mentioned|p483, p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
30422|Sunnymount Granodiorite|23423|6|Mentioned|p307 Table 7.3|||||||||
30422|Sunnymount Granodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
30422|Sunnymount Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 328. I-Type.||||||
30422|Sunnymount Granodiorite|23616|6|Mentioned|Table 3 p51|||||||||
30422|Sunnymount Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
30422|Sunnymount Granodiorite|60425|4|Described|p47 Tb. 3, p278-9 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Ste (Ootann Supste). Cuts Boxwood Volcanics (Featherbed Volcanic Gp).I-type. Three subunits: (1) med.-coarse-gr.leucogranite (2) fine- to med.-gr.biotite granite (3) med.to pale grey hornblende-biotite granodiorite - additional lith. details.||||||07-FEB-11
30422|Sunnymount Granodiorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The three variants are mapped separately.||Unit in Ootann Supersuite.|||Grey hornblende-biotite granodiorite; pink fine- to medium-grained biotite granite with numerous mafic enclaves; cream to pink, medium- to coarse-grained biotite leucogranite with quartz veins and minor tungsten-molybdenum mineralisation.|
24003|Superbus Basalt|39969|6|Mentioned|p9|||||||||
24003|Superbus Basalt|40542|6|Mentioned|p98|||||||||
24003|Superbus Basalt|40587|6|Mentioned|p361|||||||||
24003|Superbus Basalt|42485|5|Briefly described|p264|||||||||
24003|Superbus Basalt|69599|5|Briefly described|p630 Fig.8.31, p639|||Main Range volcano. Total alkalis v. SiO2 plot and discussion. Several ages for the collective Main Range lavas given.|Between ~26 Ma and ~20 Ma.||||Only mafic lava flows: basaltic (lower part), to highly alkaline in the uppermost part which commonly contains megacrysts and/or xenoliths of upper-mantle or lower-crustal material.|
24003|Superbus Basalt|73450|6|Mentioned|p92|||[Possibly a constituent of the Main Range Volcanics].||||Conformably underlain by Governors Chair Volcanics.||
24003|Superbus Basalt|73581|5|Briefly described|p7|||Southern part of the Main Range Volcano. Separated from Governors Chair Volcanics by the Streamers Trachyte and Wild Cattle Trachyandesite, the boundary is considered indistinguishable where the felsic units are absent.||||Overlies Governors Chair Volcanics||
36213|Surgeons Lookout Rhyolite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
36213|Surgeons Lookout Rhyolite|43933|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36213|Surgeons Lookout Rhyolite|43935|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
36229|Swamp Creek Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36229|Swamp Creek Granite|23624|4|Described|p11|Permian|Carboniferous|Parent: Ootann Supersuite. Intrudes the Blackman Gap Complex.||||||08-JUL-15
36229|Swamp Creek Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to grey, medium-grained, mainly even-grained biotite monzogranite, with metasedimentary inclusions.|
36229|Swamp Creek Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to grey, medium-grained, mainly even-grained biotite monzogranite, with metasedimentary inclusions.|
35201|Swayneville Granite|23042|5|Briefly described|Fig 2||Cretaceous|||||||
35201|Swayneville Granite|60473|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Of the Urannah Batholith.  Pink to red or pale grey, fine to medium grained, equigranular to slightly porphyritic granite, with variable amounts of mafic minerals.||||||
35201|Swayneville Granite|60787|5|Briefly described|p9|Cretaceous|Cretaceous|||||||
35201|Swayneville Granite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Dark pink, medium-grained, equigranular to slightly porphyritic titanite-hornblende-biotite mesogranite; commonly with inclusions of country rocks; common dark blue to green microdiorite and granodiorite as intrusions or xenoliths.||||||09-SEP-14
35201|Swayneville Granite|65388|3|Fully described|p417-418, p143, p403 Fig. 135|Cretaceous|Cretaceous|Probably Cretaceous. Intrudes Carmila beds. Two plutons. Swayneville Igneous Complex suggested as better name. Includes biotite granite to granodiorite, monzonite and monzodiorite in type area.||||||
36439|Sword Creek Microgranite|23617|4|Described|Table 2 p18|Permian|Late Carboniferous|Intrude the Wallaman Falls Volcanics. Also see p26.||||||
36439|Sword Creek Microgranite|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36439|Sword Creek Microgranite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
30647|Sybella Suite|23393|4|Described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
30647|Sybella Suite|23396|6|Mentioned|p426|||||||||
30647|Sybella Suite|23545|5|Briefly described|p605|||||||||
30647|Sybella Suite|24197|4|Described|p27, p93|Paleoproterozoic|Paleoproterozoic|Type example of Sybella Association. Series of elongate plutons and also includes Caters Bore Rhyolite. Comprises 4 main phases: main phase, quartz phase, microgranites and pegmatites; dominantly pink to grey. Age: 1670Ma. Geol.P: Mount Isa Inlier.||||||07-FEB-11
30647|Sybella Suite|24419|5|Briefly described|p17, p13 Fig.5, p14|Paleoproterozoic|Paleoproterozoic|Age: 1655-1680 Ma. Includes the Sybella Granite, Carters Bore Rhyolite, Widgewarragranite, Gidya granite, Steeles granite, Kahko granodiorite, Briar granite, Wonomo granite and Garden Creek Porphyry.||||||07-NOV-08
30647|Sybella Suite|50100|5|Briefly described|p11, p21|Paleoproterozoic|Paleoproterozoic|Of the Sybella Batholith.  Represented in this study area by the Garden Creek Porphyry.  Age: 1670Ma.  ||||||07-NOV-08
30647|Sybella Suite|50332|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Age: 1670Ma. Intrusive granites.||||||07-FEB-11
30647|Sybella Suite|50536|5|Briefly described|p1.2, 1.4, 8.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: ~1670Ma.||||||07-NOV-08
30647|Sybella Suite|63023|5|Briefly described|p1024 Fig. 1, p1035|||Comprises Carters Bore Rhyolite, Guns Knob and Widgewarra Granites; also includes Carters Bore Rhyolite. Large body of dominantly I-type granodiorite sheets. Geological Province: Western Fold Belt.||||||15-MAR-07
30647|Sybella Suite|65396|6|Mentioned|p301|||See Sybella Granite. Considered by Budd et al. (2002) to have little or no metallogenic potential in the Mount Isa Inlier.||||||
30647|Sybella Suite|65455|6|Mentioned|p7, p8 Fig. 4|Paleoproterozoic|Paleoproterozoic|Western Fold Belt, Mount Isa region. Numerous samples in the Western Fold Belt have U contents exceeding 20 ppm.||||||09-MAY-12
30647|Sybella Suite|66529|5|Briefly described|p60, p67, p94 |||Northern part contains moderate to highly prospective granitoids for orthomagmatic U deposits.||||||
30647|Sybella Suite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p41|Statherian|Statherian|See also p107. Sybella Batholith age tightly constrained between 1675 and 1670 Ma. CONSTITUENTS (continued): Yarrie Rock Waterhole Granite; Garden Creek Porphyry, Kahko Granodiorite, Kitty Plain Microgranite.|||Annable, Briar, Copper Valley, Easter Egg, Gidya, Gunns Knob, Hay Mill, Keithys, Lithgow, Nobbs Tank, Queen Elizabeth, Steeles, Sybella, Templeton, Widgewarra, Wonomo Granites. See COMMENTS for more.|Carters Bore Rhyolite also related to this event.||
30647|Sybella Suite|68542|6|Mentioned|p1 |||||||||
30647|Sybella Suite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
30647|Sybella Suite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
30647|Sybella Suite|69591|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|||||||
30647|Sybella Suite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Shown as older than the Isan Orogeny (1590-1500 Ma).|||Includes Garden Creek Porphyry.|Shown as partially age equivalent to Surprise Creek Formation.|Porphyritic microgranite.|
30647|Sybella Suite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Shown as older than the Isan Orogeny (1590-1500 Ma).|||Includes Garden Creek Porphyry.|Shown as partially age equivalent to Surprise Creek Formation.|Porphyritic microgranite.|
30647|Sybella Suite|72889|6|Mentioned|p6 Fig.i.|||||||||
30647|Sybella Suite|73413|6|Mentioned|p3|Statherian|Statherian|Mount Isa Inlier, Western Fold Belt.|1675-1655 Ma|||||
30647|Sybella Suite|73529|6|Mentioned|p15 Fig.11|Statherian|Statherian||1670-1655 Ma|||||
26155|Sybil Group|23422|4|Described|p183, p204 Table 6.3|Late Carboniferous|Late Carboniferous|Maximum thickness: ~1600m.||||||
26155|Sybil Group|23424|5|Briefly described|Fig 8.4|Permian|Carboniferous|||||||
26155|Sybil Group|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
26155|Sybil Group|23893|5|Briefly described|p18|Early Permian|Late Carboniferous|||||||
26155|Sybil Group|24612|5|Briefly described|p9 Fig.2|Early Permian|Late Carboniferous|Geological Province: Burdekin Basin.||||||06-APR-05
26155|Sybil Group|24613|5|Briefly described|p6 Fig. 3, p109|Early Devonian|Precambrian|Geological province: Burdekin Basin. Ewan group is faulted against this unit.||||||07-FEB-11
26155|Sybil Group|32169|6|Mentioned|Table 2|||U.Carb.||||||
26155|Sybil Group|37573|6|Mentioned|p225|||See also Fig.2||||||
26155|Sybil Group|37613|6|Mentioned|p249|||See also Fig.3||||||
26155|Sybil Group|39445|6|Mentioned|Table 7|||||||||
26155|Sybil Group|41120|6|Mentioned|p196|||||||||
26155|Sybil Group|41735|6|Mentioned|p284|||||||||
26155|Sybil Group|41774|6|Mentioned|p31|||||||||
26155|Sybil Group|41916|6|Mentioned|p28|||||||||
26155|Sybil Group|42031|6|Mentioned|Fig.6 P763|||||||||
26155|Sybil Group|42295|5|Briefly described|Fig.2 P5|||||||||
26155|Sybil Group|42547|5|Briefly described|p76|||||||||
26155|Sybil Group|42690|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
26155|Sybil Group|42692|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
26155|Sybil Group|42752|5|Briefly described|Fig.2 P46|||||||||
26155|Sybil Group|42933|5|Briefly described|Fig.6|||||||||
26155|Sybil Group|43095|1|Redefined|p66|||||||||
26155|Sybil Group|43259|6|Mentioned|Appendix 1,p6.||Carboniferous|Late Carboniferous? in age.||||||
26155|Sybil Group|43589|6|Mentioned|p16 (map legend), p21||Late Carboniferous|Macauley Creek Granite is faulted against this group.||||||23-APR-08
26155|Sybil Group|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
26155|Sybil Group|44061|4|Described|Table 3||Late Carboniferous|||||||
26155|Sybil Group|44091|14|Not recorded|p40|Late Carboniferous|Early Carboniferous|(M.Carb - L.Carb)||||||
26155|Sybil Group|45097|6|Mentioned|p22|||Part equivalent of Treela Volcanics. Correlation chart.||||||
26155|Sybil Group|48904|2|Defined|p39|Late Carboniferous|Late Carboniferous|See also p40.||||||23-APR-08
26155|Sybil Group|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Charters Towers Province.||||||
26155|Sybil Group|68350|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.|||Includes Hells Gate Rhyolite and Marshs Creek Formation.|||
26155|Sybil Group|68351|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.|||Includes Hells Gate Rhyolite and Marshs Creek Formation.|||
26155|Sybil Group|68731|6|Mentioned|p203, p223 Fig 3.126|Cisuralian|Pennsylvanian|Comprises terrestrial volcanics and sediments.||||||18-JUL-14
26155|Sybil Group|69592|5|Briefly described|p274 Fig.4.65, p275-276|Permian|Pennsylvanian|Wyatt et al. (1970); Gunther and Withnall (1992). Sybil Graben. Covers rocks of the Charters Towers Province and Camel Creek Subprovince. ~1.5km thick; tilted to gently folded.|||Hells Gate Rhyolite, Marshs Creek Formation, Wade beds.|Is faulted against Macauley Creek Granite. Correlative with Wade beds.||
26155|Sybil Group|69593|5|Briefly described|p495-496|Permian|Late Carboniferous|NW-trending Sybil Graben, Townsville hinterland. Younger age may be Late Carboniferous.|||Hells Gate Rhyolite.||Crystal-rich rhyolitic ignimbrite, rhyolite lava, volcaniclastic and epiclastic rocks, and other sediments; minor mafic rocks.|
26157|Tadpole Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
26157|Tadpole Granite|22781|4|Described|p30|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
26157|Tadpole Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Coen Metamorphic Group. Intruded by Burns Granite and Ebagoola Granite.||||||
26157|Tadpole Granite|42610|2|Defined|p15|Early Devonian|Early Devonian|Reserved as Tadpole Monzogranite. Age assumed approx 400Ma. Included in "Kintore Adamellite" of B135||||||
26157|Tadpole Granite|43738|6|Mentioned|Fig.12,p38|||||||||
26157|Tadpole Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
26157|Tadpole Granite|71849|3|Fully described|p2-3, p8, p15, p57-58, p60, p81-84, p89|Devonian|Devonian|See also p147, p150, p155, p157-158, p183-184, p195. Coen Inlier. Forms a narrow (~8km x ~1km wide) NW-trending belt. Defined and included in Ebagoola Suite by Mackenzie and Knutson (1992); previously included in the Kintore Adamellite. Deeply weathered and very poorly exposed. In and adjacent to Ebagoola Shear Zone: extensively deformed and recrystallised, locally foliated. Geophysics briefly described. Lithology detailed; photomicrographs.?Post-dates Vardon Granite. Not isotopically dated; member of Pama Igneous Association implies intrusion between c.415-395 Ma.||Ebalooga Suite.||Intrudes Yarraden Schist.|S-type. White to pale grey or pale bluish-grey, medium-grained, moderately porphyritic (garnet-)muscovite-biotite monzogranite with K-feldspar and plagioclase phenocrysts. Minor to trace garnet, rare sillimanite and altered cordierite.|
26157|Tadpole Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Mid to pale grey garnet-bearing biotite granite, mostly foliated.|
29966|Takura beds|24382|5|Briefly described|Map legend|Oligocene|Eocene|||||||
29966|Takura beds|43059|4|Described|Table 2|||see also p10||||||
29966|Takura beds|60281|5|Briefly described|p38, Fig 30 App 1|Early Miocene|Late Eocene|Thin, colluvial deposits - sandstone, conglomerate, siltstone.  Facies equivalents of the Elliot Formation. Max. thickness: 52m.  Geological Province: edges of the Maryborough Basin.||||||
29966|Takura beds|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|Thickness, together with Elliott Formation: 50m. In the Bundaberg-Maryborough region. ||||||
29966|Takura beds|63821|5|Briefly described|p25|Tertiary|Tertiary|Max. thickness: 10m. Scree deposits derived from silicified mudstone at top of Maryborough Formation - comprising poorly sorted oligomictic conglomerate and rubble breccia.||||||07-FEB-11
29966|Takura beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
29966|Takura beds|69599|5|Briefly described|p586-587|Oligocene|Eocene|Capricorn Basin. Crops out as a series of ridges east of Maryborough. Up to 10m thick. Capped by laterite and silcrete. RELATED UNITS (continued): Also correlated (at least partly) with Beaudesert, Pomona, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; Flinders Dolomite; Oakdale Sandstone.||||Overlies Fairymead beds; also Maryborough Formation and Burrum Coal Measures unconformably. Correlated (at least partly) with Elliott, Petrie and Lowmead Formations; see COMMENTS for more.|Conglomerate and breccia with locally derived clasts of Maryborough Formation.|
29597|Talamy Schist|22845|2|Defined|p13,18,25-7,77|Early Carboniferous|Late Devonian|Probably correlates with Murdering Creek Metamorphics.||||||
29597|Talamy Schist|22846|6|Mentioned|p37||Late Permian|||||||
29597|Talamy Schist|43588|6|Mentioned|p30||Late Devonian|||||||
29597|Talamy Schist|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
29597|Talamy Schist|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||09-JUN-04
29597|Talamy Schist|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
29597|Talamy Schist|68679|5|Briefly described|p325-326, p328-329|||Little (1993) mapped this unit as quartz-mica schist inclusions (as blocks and slabs 1-3000m thick) within Mount Mia Serpentinite. Kilkivan-Manumbar area, North D'Aguilar Subprovince. Lower plate accretionary assemblage. Experienced two-phase metamorphic/structural history (subduction and exhumation).||||Occurs within Mount Mia Serpentinite. Correlative of Gobongo Metamorphics.|Quartz-mica schist, metaquartzite (probably metachert), and albite-rich schist that locally grades into mafic blueschist-greenschist of the Mount Mia Serpentinite.|
27654|Talaroo Microgranite|23291|5|Briefly described|p97 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Newcastle Range I-types. Geological Province: Georgetown Region.||||||29-MAY-15
27654|Talaroo Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
27654|Talaroo Microgranite|40542|6|Mentioned|p97|||||||||
27654|Talaroo Microgranite|43259|4|Described|Appendix 1,p16.||Carboniferous|||||||
27654|Talaroo Microgranite|43740|4|Described|p16|||||||||
27654|Talaroo Microgranite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
27654|Talaroo Microgranite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to brown and pink, abundantly porphyritic biotite-hornblende microgranite.|
27654|Talaroo Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Newcastle Range Volcanic Group.|||||I-type: biotite microgranite and granite.|
24007|Talaveras Rhyolite|23291|5|Briefly described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Agate Creek Volcanic Group. Geological Province: Georgetown Region.||||||25-MAY-15
24007|Talaveras Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V32. I-Type.||||||
24007|Talaveras Rhyolite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
24007|Talaveras Rhyolite|40542|6|Mentioned|p97|||||||||
24007|Talaveras Rhyolite|40860|5|Briefly described|p115|||||||||
24007|Talaveras Rhyolite|43259|4|Described|Appendix 1,p3.||Permian|of Agate Creek Volcanic Group.||||||
24007|Talaveras Rhyolite|43740|4|Described|p30, 78||Carboniferous|Includes data on contacts & thickness.||||||01-SEP-04
24007|Talaveras Rhyolite|50199|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Agate Creek Volcanic Group.||||||
24007|Talaveras Rhyolite|50211|4|Described|Map Legend|Early Permian|Early Permian|Of Agate Creek Volcanic Group. Overlain by Black Soil Andesite. Overlies Big Surprise Tuff. Rhyolitic ignimbrite with sparse biotite and lithic clasts.||||||14-MAY-04
24007|Talaveras Rhyolite|68353|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Conformably overlies Big Surprise Tuff. Is overlain conformably by Black Soil Andesite.|Reddish brown rhyolitic ignimbrite with sparse biotite and lithic clasts.|
24007|Talaveras Rhyolite|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Conformably overlies Big Surprise Tuff. Is overlain conformably by Black Soil Andesite.|Reddish brown rhyolitic ignimbrite with sparse biotite and lithic clasts.|
36729|Talgijah Granodiorite|23423|5|Briefly described|p252|||Of Yates Supersuite.||||||
36729|Talgijah Granodiorite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Yates Supersuite. Geological Province: Kennedy Province.||||||
36729|Talgijah Granodiorite|60425|4|Described|p91, p272-3 Appdx. 1|Early Permian|Early Permian|Of Talgijah Suite (Yates Supersuite). I-type. Fine-med..gr, even-gr.to sightly porph.hornblende?-biotite granodiorite to diorite? with numerous biotite-rich enclaves. Garnet xenocrysts present. For further lithological detail - see p273.||||||07-FEB-11
36729|Talgijah Granodiorite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Yates Supersuite.||||
69327|Talgijah Suite|60425|5|Briefly described|p272-3 Appdx. 1|Early Permian|Early Permian|Of Yates Supersuite. Contains Talgijah Granodiorite. I-type.||||||07-FEB-11
35192|Tally Ho Igneous Complex|23042|4|Described|p96,7, Fig 2||Late Carboniferous|||||||
35192|Tally Ho Igneous Complex|60445|6|Mentioned|p29, p31 Tb. 9|||Contains greisen bodies.||||||
35192|Tally Ho Igneous Complex|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35192|Tally Ho Igneous Complex|65388|2|Defined|p384-385, 370,376, 380, 392, 399|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Surrounds Mount Shields Granodiorite. Intruded by Whitehorse Granite. Other relationships not clear. Tentative age given.The oldest parts consist of diorite and granodiorite, locally sheared or foliated; intruded by and included as enclaves in the more abundant hornblende-biotite granodiorite and granite; aplite and pegmatite intrude all earlier phases. Shown as Tally Ho Complex on p399.||||||
35192|Tally Ho Igneous Complex|73197|6|Mentioned|p471|Guadalupian|Late Carboniferous|New England Orogen, northern. Shown as Tally Ho igneous complex. See also misspelling Tallyho Igneous Complex p470.|||||Predominantly I-type granitoids, includes small S-type granitoid phases.|
36189|Tam O'Shanter Granite|23423|5|Briefly described|p225||Ordovician|Also see p262. Macrossan Province.||||||
36189|Tam O'Shanter Granite|23497|5|Briefly described|Table 1|Late Ordovician|Early Ordovician|of Macrossan Province. Age: 486+/-10Ma (U-Pb zircon SHRIMP). Intrudes Barnard Metamorphics.||||||
36189|Tam O'Shanter Granite|23507|5|Briefly described|Map Legend||Early Ordovician|Age: 486+/-10Ma SHRIMP.||||||
36189|Tam O'Shanter Granite|60425|5|Briefly described|p6, p8, p10|Early Ordovician|Cambrian|Intruded Barnard Metamorphics. Age: 486+/-10Ma. S-type. Occur at Tam O'Shanter Point, Qld. See also p115.||||||07-FEB-11
36189|Tam O'Shanter Granite|68731|5|Briefly described|p159, p162|Early Ordovician|Paibian|Another sample from this granite was analysed, yielding a U-Pb zircon (LA-ICP-MS) age of 455.7 +/- 3.6 Ma.|485 +/- 7 Ma, U-Pb SHRIMP (Bultitude et al. 1999)|||Extensively intrudes the Barnard Metamorphics.||
36189|Tam O'Shanter Granite|69030|5|Briefly described|p6|Ordovician|Ordovician|Barnard Province.|455.7 +/- 3.6 Ma (SHRIMP).||||I-type granitoids.|
36189|Tam O'Shanter Granite|70033|5|Briefly described|p5, p52 Fig 8.1, p61|Ordovician|Ordovician|BB1716; 445.7 +/- 3.6 Ma; LA-ICPMS; R.Wormald, James Cook University, pers. Comm. June 2011; see Bultitude and Champion 2013.||||Intrudes Barnard Metamorphics.||
36189|Tam O'Shanter Granite|70207|5|Briefly described|p1, p52|||Thomson Orogen.|455.7 +/- 3.6 Ma (Bultitude and Champion, 2013).|||Intrudes Barnard Metamorphics.||
36189|Tam O'Shanter Granite|73425|6|Mentioned|p16|Late Ordovician||Barnard Province, Thomson Orogen.||||||
75141|Tam O'Shanter Supersuite|60425|3|Fully described|p62 Tb. 4|Early Ordovician|Early Ordovician|Contains Tam O'Shanter Granite. Age: 486+/-10Ma (SHRIMP). Intruded Barnard Metamorphics. Medium-grained, even-grained to slightly porphyritic (altered cordierite?-) muscovite-biotite granite with numerous enclaves of biotite gneiss and quartz; S-type.||||||07-FEB-11
26160|Tamaree Formation|23251|5|Briefly described|Table 1 p12, p20|Late Permian|Permian|Age: may range into the Early Triassic. Fossil assemblage include shells of Late Permian age. Gympie Group. Kin Kin Subprovince, Gympie Province. Overlying unit Keefton Formation. Underlying unit South Curra Limestone.||||||30-NOV-05
26160|Tamaree Formation|23542|4|Described|p380|||Of the Gympie Group.||||||22-OCT-08
26160|Tamaree Formation|23799|6|Mentioned|p34|||||||||
26160|Tamaree Formation|24078|5|Briefly described|p425 Tb. 1|Late Permian|Late Permian|Thin, lithic subgreywacke, green grey shales.  Max. thickness: 670m.  Geological Province: Gympie Basin.||||||
26160|Tamaree Formation|30450|6|Mentioned|Table 1|||Permian age. Maryborough Basin||||||
26160|Tamaree Formation|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
26160|Tamaree Formation|31703|6|Mentioned|Table|||P4||||||
26160|Tamaree Formation|34475|2|Defined|p258|Late Permian|Late Permian|||||||
26160|Tamaree Formation|35101|5|Briefly described|p31|||||||||
26160|Tamaree Formation|37400|6|Mentioned|Table 2|||||||||
26160|Tamaree Formation|39252|6|Mentioned|p22|||See also p28 and Fig.13||||||19-SEP-17
26160|Tamaree Formation|39261|6|Mentioned|p112|||||||||
26160|Tamaree Formation|39284|5|Briefly described|p431|||||||||
26160|Tamaree Formation|39445|5|Briefly described|Table 8|||See also Table 9||||||
26160|Tamaree Formation|41157|6|Mentioned|Fig.1|||||||||
26160|Tamaree Formation|41736|6|Mentioned|p120|||||||||
26160|Tamaree Formation|41917|6|Mentioned|p526|||||||||
26160|Tamaree Formation|42450|5|Briefly described|p404, p405|||||||||
26160|Tamaree Formation|42751|4|Described|p24|||of Gympie Group||||||
26160|Tamaree Formation|43017|6|Mentioned|p380|||||||||
26160|Tamaree Formation|43100|4|Described|p28|Early Triassic|Permian|of Gympie Group.||||||
26160|Tamaree Formation|44928|5|Briefly described|Map Legend||Permian|||||||
26160|Tamaree Formation|60330|6|Mentioned|p261|||||||||
26160|Tamaree Formation|61780|4|Described|p258, p256||Triassic|Thickness: >600m. Graded, rhythmically bedded arenite, siltstone, shale; carbonaceous, pyritic, calcareous (turbidites distal to shoreline, anoxic).||||||
26160|Tamaree Formation|65380|5|Briefly described|p671|Late Permian|Late Permian|Includes only sparse fossils.||Topmost unit of Gympie Group||Overlain by Keefton Formation.||
26160|Tamaree Formation|68679|5|Briefly described|p369-370|Wuchiapingian|Wuchiapingian|Runnegar and Ferguson (1969). Southern Gympie Province. 800m thick. Contains a Wuchiapingian fauna.||Gympie Group.||Overlies the South Curra Limestone. Is overlain unconformably by Keefton Formation. Correlated with Teebar Formation.|Sandstone, siltstone, carbonaceous shale, rhythmically bedded turbidites dominated by volcanic lithic fragments with rare conglomerates; cross-bedding, load casts and flame structures common; poorly fossiliferous.|
26160|Tamaree Formation|70913|1|Redefined| p14-16, p1, p8 fig 3, p9, p12 fig 4,|Late Permian|Middle Permian|Gympie Province. Name derived from Tamaree Railway Station, north of Gympie. Type section and drill section mentioned. Lithology discussed in detail, including sedimentary structures and mineralogy. Thickness in the type section is around 670m. Fossil assemblage discussed. Previously included as part of the Upper Gympie Formation. See also p7, p67 fig 9, p76, p80, maps in Appendix 1. .|255 to 265 Ma (U-Pb detrital Zr, Li et al, 2015)|Gympie Group||Conformably overlies the South Curra Limestone. Conformably overlain by Keefton Formation in places.|Rhythmically graded interbeds of arenite, siltstone and mudstone that fines upwards to bioturbated siltstone, shale and mudstone.|15-SEP-17
26160|Tamaree Formation|72037|4|Described|p859,861-866,870|Late Permian|Late Permian|Geological province: New England Orogen, Gympie Terrane. Depositional environment: distal to shoreline turbidites. LA-ICP-MS peak detrital zircon U-Th-Pb ages include 255, 299, 312, and 333 Ma. Maximum depositional age at c. 255 Ma; deposition constrained to late Permian based on c. 258 Ma tuff in the underlying South Curra Limestone. Late Permian to Triassic detrital zircons likely sourced from a middle Permian to Triassic continental arc system to the west, which was built on the former accretionary complex of the New England Orogen Gust et al., 1993; Bryant et al., 1997; Holcombe et al., 1997b; Li et al., 2012b).Carboniferous-age zircons correspond to detritus eroded from a Carboniferous magmatic arc of the New England Orogen, or recycled through the Carboniferous fore-arc and accretionary complex rocks.||||Underlain conformably by South Curra Limestone.|Rhythmically bedded sandstone, siltstone, and mudstone.|
26160|Tamaree Formation|73303|5|Briefly described|p61 Fig.2, p62, p68 Fig.9, p69|Lopingian|Lopingian|New England Orogen. Gympie Terrane, southern. Shallow marine shelf depositional environment with sediment derived from Carboniferous sources in New England Orogen.|255 Ma detrital zircon maximum depositional age|||Overlies South Curra Limestone, underlies Keefton Formation.|Rhythmically bedded marine siliciclastic sandstone-siltstone beds.|
41792|Tanderra Volcanics|60479|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes: Charons Point Rhyolite Member. Rhyolitic Ignimbrite, andesitic and basaltic lava, volcaniclastic sandstone and conglomerate; minor dacitic lava and tuff.||||||29-SEP-04
41792|Tanderra Volcanics|60481|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Andesitic and basaltic lava and moderatly to poorly-sorted volcaniclastic sandstone and conglomerate; minor dacitic lava and tuff.||||||
41792|Tanderra Volcanics|61035|4|Described|p12|Early Carboniferous|Late Devonian|Overlain by Glenprairie beds. Age: 352Ma (SHRIMP). Geological Province: Yarrol Province. Oldest unit in area. Consists of andesitic and basaltic lava and volcaniclastic sandstone and conglomerate with minor dacitic lava and volcaniclastics.||||||07-FEB-11
41792|Tanderra Volcanics|65388|3|Fully described|p69-73; 70, 58, 66-67, 68, 75, 77, 92|Early Carboniferous|Late Devonian|Of Campwyn Subprovince, Yarrol Province. Includes Charon Point Rhyolite Member. Unconformably overlain by Glenprairie beds. Equivalent age to Campwyn Volcanics. Correlated with Mount Alma or Balaclava Formations in Sth. Previously mapped as Carmila beds. Base is not exposed, so complete section cannot be given for the unit. Mainly andesitic or basaltic lavas and volcaniclastic sedimentary rocks and generally minor felsic rocks apart from a major development of rhyolitic ignimbrite at Charon Point. See also p443, 445, 447||||||
41792|Tanderra Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Balaclava, Lochenbar and Mount Hoopbound Formations, the Channer Creek beds and Three Moon Conglomerate, are all mapped under the symbol, DCa.||||||
41792|Tanderra Volcanics|68679|5|Briefly described|p308, p312-313, p338, p346-349, p359|Early Carboniferous|Late Devonian|Withnall et al. (2009). Crops out between Tanderra homestead and Charon Point; airborne magnetic data indicates it extends N under Broad Sound. Campwyn Subprovince, Yarrol Province. Stoodleigh Subprovince, Northern Yarrol Province. Similar age to Campwyn Volcanics and similar chemistry to Lochenbar Formation. Mainly subaerial deposits by fluvial debris flows.|||Charon Point Rhyolite Member.|May correlate with Campwyn Volcanics and Mount Alma or Balaclava Formations.|Mainly andesitic or basaltic lavas, aphyric to porphyritic, locally amygdaloidal; mafic volcaniclastic sediments, mostly thick-bedded and massive sandstone to pebble conglomerate or breccia; siltstone and mudstone; felsic rocks are minor.|
41792|Tanderra Volcanics|73197|5|Briefly described|p465 Fig.4, p467|Carboniferous|Carboniferous|New England Orogen, northern. Campwyn Subprovince. Forearc basin with extensive arc-proximal rocks.|||||Basaltic lavas and silicic tuffs and ignimbrites.|
69004|Tandora Granodiorite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Medium to coarse-grained, equigranular, pale grey, titanite-bearing hornblende-biotite granodiorite; very coarse-grained pale grey to pink, equigranular biotite syenogranite.||||||
69004|Tandora Granodiorite|65388|2|Defined|p331-332, 310, 301, 303, 304,318,327,340|Early Triassic|Late Permian|New name in Rawbelle area. Of Tandora Suite. Includes rocks formerly considered part of Culcraigie Granite and Wingfield Adamellite. Excludes rocks now mapped as Greystone Granodiorite. Mapped in contact with Culcraigie Granite,Telemark Granodiorite. Relationships masked by cover. Age inferred. Dominantly granodiorite, but also incorporates syenogranite, leucogranite, monzogranite, diorite, quartz diorite and gabbro. May need subdivision in future.||||||
69004|Tandora Granodiorite|68679|5|Briefly described|p419-420|||Rawbelle Batholith. ~50 km2. Separated from Culcraigie Granite by radiometric interpretation and more diverse lithology that suggest it may not be a single unit. Geochemistry plot. Age and relationships uncertain.||Tandora Suite.|||Hornblende-biotite granodiorite; biotite syenogranite.|
77828|Tandora Suite|65388|4|Described|p281-284, 287, 295-298, 300, 318, 333|Early Triassic|Late Permian|Rawbelle Batholith. I-type. Includes Cadarga Creek, Flat Range, Impey, Kildare, Tandora, Telemark, Aisbetts Granodiorites, Culcraigie, Wathonga, East Apple, Morrow Granites. Geochemistry compared with Tecoma Granite. Some samples of Wingfield Granite plot in this Suite too. See also p338, 339-340, 447.||||||
77828|Tandora Suite|68553|6|Mentioned|Map legend; schematic diagram.|Early Triassic|Late Permian|This unit, as well as the Harrami Igneous Complex, the Wingfield Suite, the Delubra Gabbro, and various unnamed plutonic units in the Rawbelle Batholith, are all mapped under the symbol, PRgr.||||||30-SEP-15
77828|Tandora Suite|68679|5|Briefly described|p312, p416, p418-420|Early Triassic|Permian|Withnall et al. (2009). Rawbelle Batholith, northern New England Orogen. Geochemistry plot.|||Aisbetts, Cadarga Creek, Flat Range, Impey, Kildare, Tandora, Telemark Granodiorites; Culcraigie, East Apple, Morrow, Wathonga Granites.|Is intruded by Aisbetts Granodiorite.||
24512|Tangalooma Sandstone|12597|5|Briefly described|p496|||Mimosa Syncline area, Clarence-Moreton Basin. Up to 200m thick.||Unit in Walloon Coal Measures.|||Lithic and feldspathic labile sandstone with a carbonate cement; upward-fining sequences common; local thin coal lenses.|
24512|Tangalooma Sandstone|37993|3|Fully described|p162|||||||||
24512|Tangalooma Sandstone|38658|6|Mentioned|p153|||||||||
24512|Tangalooma Sandstone|40675|6|Mentioned|Table 9A|||||||||
24512|Tangalooma Sandstone|60993|5|Briefly described|p34|||Name probably obsolete now?  A barren sand occurring in the middle unit of their Walloon "Subgroup" between the coal-bearing intervals above and below. Geol. Prov: northeastern Surat Basin into the Clarence-Moreton Basin. ||||||28-AUG-12
24512|Tangalooma Sandstone|63218|6|Mentioned|p211 Fig.2, p212 Fig.3. |Middle Jurassic|Middle Jurassic|Surat Basin. The article details analyses for coal seam gas.||Unit in Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Juandah Coal Measures.||
24512|Tangalooma Sandstone|64665|5|Briefly described|p61.|Middle Jurassic|Middle Jurassic|Surat Basin. Is said to separate the Taroom and Juandah Coal Measures, but does not say which of these is the upper or lower unit.||Unit in Walloon Subgroup.||||
24512|Tangalooma Sandstone|64856|5|Briefly described|p87|Middle Jurassic|Middle Jurassic|Of the Walloon Coal Measures (Subgroup) of Jones and Patrick (1979). Middle Jurassic age implied.| | ||||31-JAN-13
24512|Tangalooma Sandstone|65096|5|Briefly described|p372, p368, p370 Fig.2, |Middle Jurassic|Middle Jurassic|Jones and Patrick (1981). Up to 40 m thick.  Lenticular and easy to misidentify on wireline logs since each coal sequence generally begins with a sandstone bed of variable thickness . Equivalent to the basal part of the Argyle Seam Package.||Of the Walloon Coal Measures/Walloon Subgroup.||Underlain by the Taroom Coal Measures. Overlain by the Juandah Coal Measures.|Commonly appears as an upper and lower sandstone separated by a shale layer which often includes a coal seam.|
24512|Tangalooma Sandstone|67133|5|Briefly described|p12-14|||Illite-rich mixed-layer clays.||Walloon Subgroup.||||
24512|Tangalooma Sandstone|68117|4|Described|p345-350, p353, p355|Middle Jurassic|Middle Jurassic|Jones and Patrick (1981) after Swarbrick (1973)'s interval 6 of Injune Creek Group. Now recognised across entire eastern Surat Basin. 10-100m thick. The base is the top of the Auburn Seam or, where that is absent, the base of the first major channel-sand deposit above the argillaceous interval representing the Auburn Seam. The top is the base of the Argyle Seam.||Walloon Subgroup.||Conformably overlies Taroom Coal Measures. Is overlain conformably by Juandah Coal Measures.|Light grey to grey, fine- to medium-grained labile sandstone with argillaceous matrix; comprises two or three upward-fining sequences, which culminate in siltstone, mudstone and rarely coal.|
24512|Tangalooma Sandstone|68139|5|Briefly described|p21, 24-33|Middle Jurassic|Middle Jurassic|Surat Basin. Maceral composition tabulated, discussed. May form a regional-scale barrier to gas migration from below, and to biogenic and meteoric recharge from above.||Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Lower Juandah Coal Measures.|Mainly sandstone; minor coal.|
24512|Tangalooma Sandstone|69574|5|Briefly described|p21-24, 26-32, 35|Middle Jurassic|Middle Jurassic|Surat Basin. Desorbed gas molecular composition and compound-specific isotopes tabulated.||Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Lower Juandah Coal Measures.|Contains minor coal.|
24512|Tangalooma Sandstone|69594|6|Mentioned|p536|||Jones and Patrick (1981) raised the Walloon Coal  Measures to Subgroup status and included this unit, as well as the Taroom and Juandah Coal Measures. In this study, they are regarded as Members of the Walloon Coal Measures only in the NE Surat Basin.||||||
24512|Tangalooma Sandstone|69790|5|Briefly described|p1061, p1065-1077|||Jones and Patrick (1981). Thins to the S.||Unit in Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Juandah Coal Measures.||
24512|Tangalooma Sandstone|70374|5|Briefly described|p808, p809 figure 1, p811|Oxfordian|Oxfordian|||Walloon Coal Measures /Walloon Subgroup.||Overlies Taroom Coal Measures, underlies Juandah Coal Measures or Maclean Sandstone Member.||28-SEP-16
24512|Tangalooma Sandstone|70628|6|Mentioned|p952,964,965 Fig 17|Bathonian|Bathonian|Previously believed to be a regionally correlatable sand sheet, but new drilling shows that it is not pervasive and likely diachronous where present.||Walloon Subgroup||Overlies Taroom Coal Measures, underlies Juandah Coal Measures.|Sandstone.
|30-JUN-16
24512|Tangalooma Sandstone|70725|5|Briefly described|p11, 13-14, 16-19, 22, 24-25|Late Jurassic|Late Jurassic|Surat Basin. Maceral composition and vitrinite reflectance graphed and discussed. 13C isotope vs. depth tabulated.||Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Lower Juandah Coal Measures.|Sandstone with few thin coal seams.|
24512|Tangalooma Sandstone|71282|5|Briefly described|p456, p457 Fig.1, p460, p466 Fig.13|||Jones and Patrick (1981). Surat Basin. [The authors of this article incorrectly state that Jones and Patrick "informally" named this unit.] See also p467-468.||Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Juandah Coal Measures.||
24512|Tangalooma Sandstone|72297|5|Briefly described|p699, p751|Jurassic|Jurassic|NE Surat Basin. Elsewhere this is part of the Walloon Coal Measures.||Walloon Subgroup.||Overlies Taroom Coal Measures. Is overlain by Juandah Coal Measures.||
26282|Tank Creek Sandstone|23032|5|Briefly described|p27 fig6||Early Devonian|||||||
26282|Tank Creek Sandstone|23424|5|Briefly described|Table 8.1|Givetian|Emsian|Of Wando Vale Subgroup/Broken River Group, Graveyard Creek Subprovince.||||||
26282|Tank Creek Sandstone|23522|5|Briefly described|p250 Fig 6|Emsian|Emsian|||||||
26282|Tank Creek Sandstone|24577|5|Briefly described|p754 Fig. 2|Devonian|Devonian|Of the Broken River Group. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
26282|Tank Creek Sandstone|41260|4|Described|Table 1|||Briefly described P188||||||
26282|Tank Creek Sandstone|41679|2|Defined|p255|Emsian||||||||
26282|Tank Creek Sandstone|41739|6|Mentioned|Fig.2|||||||||
26282|Tank Creek Sandstone|41740|6|Mentioned|p222|||||||||
26282|Tank Creek Sandstone|42031|5|Briefly described|Fig.5 P762|||||||||
26282|Tank Creek Sandstone|42032|6|Mentioned|Fig.12 P505|||||||||
26282|Tank Creek Sandstone|42054|6|Mentioned|p273|||||||||
26282|Tank Creek Sandstone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
26282|Tank Creek Sandstone|42933|3|Fully described|Table 2|||See also p79||||||
26282|Tank Creek Sandstone|50093|5|Briefly described|p329 Fig.2|Emsian|Emsian|Overlain by Chinaman Creek Limestone. Of Broken River Group.||||||07-FEB-11
26282|Tank Creek Sandstone|65214|6|Mentioned|p275|Devonian|Devonian|QLD, Broken River. Appears in text as Tank Ck Sandstone. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
26282|Tank Creek Sandstone|68336|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Coarse-grained quartzose sandstone and minor fine-grained lithic sandstone.|
26282|Tank Creek Sandstone|68341|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Coarse-grained quartzose sandstone and minor fine-grained lithic sandstone.|
26282|Tank Creek Sandstone|69592|5|Briefly described|p264-265|Early Devonian|Early Devonian|Pandanus Creek area; Graveyard Creek Subprovince, Broken Creek Province. Up to 80m thick. Marine fossils; shoreline deposits.||Basal Wandovale Subgroup.|||Coarse, locally pebbly, quartzose sandstone grading upwards into fine- to medium-grained lithic sandstone. Trough and planar cross-lamination are widespread; sporadic, pooorly preserved macrofossils.|
29045|Tannum Sands|35043|6|Mentioned|p78|||||||||
29045|Tannum Sands|36211|6|Mentioned|p267|||||||||
29045|Tannum Sands|41538|6|Mentioned|p305|||||||||
75143|Tapp Ana Suite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of the Tapp-Ana Supersuite. Contains the informally named Tapp-Ana granite. S-type?||||||07-FEB-11
75142|Tapp Ana Supersuite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Contains the Tapp-Ana Suite. S-type?||||||07-FEB-11
75144|Tapp Ana granite|60425|4|Described|p100, p288-9 Appdx. |Early Carboniferous|Early Carboniferous|Informal name for S-type(?) granite (SW side of Dunk Island). Medium- to coarse-grained, moderately porphyritic biotite granite; with rare ovoid pegmatitic zones; a well-dev'd tectonic foliation + numerous enclaves - more lithological detail included||||||07-FEB-11
38894|Targinie Quartz Monzonite|24420|4|Described|p8|Late Triassic|Late Permian|||||||
38894|Targinie Quartz Monzonite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgta].  Pink, medium-grained hornblende-biotite quartz monzonite.||||||
38894|Targinie Quartz Monzonite|50207|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
38894|Targinie Quartz Monzonite|68008|4|Described|p160, p424-426|Triassic|Permian|Originally the Targinie Adamellite of Kirkegaard et al. (1970). Chemical analysis shows it is a quartz monzonite rather than a monzogranite. Yarwun district. A N-S elongate intrusion, 10 x 3 km, centred 15km WNW of Gladstone. Some small outcrops W of the main body. Has varied topographic expression (described). Geophysics and geochemistry described. Age unknown: assumed to be like most local intrusives. Hosts and is source of several gold-bearing reefs.||||Intrudes the Balnagowan Volcanic Member and the Berserker Group.|Medium-grained granitoid comprising microperthite (>40%), sodic andesine (<35%), quartz (<15%), biotite and hornblende (together 10%), minor opaques and accessory apatite and zircon. Altered to quartz and alunite to form the peak at Mount Larcom.|
38894|Targinie Quartz Monzonite|68679|5|Briefly described|p425|||Yarrol Province. An elongate N-S, ~10km-long intrusion near Mount Larcom.||||Intrudes Balnagowan Volcanic Member and parts of the Berserker Group.|Hornblende-biotite quartz monzonite. Contains conspicuous "plug" of quartz-alunite alteration.|
24011|Taroborah Granodiorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37.||||||
24011|Taroborah Granodiorite|43029|2|Defined|p22||Middle Devonian|see also Fig.2,p16||||||
24011|Taroborah Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Taraborah Batholith||||||23-DEC-11
24011|Taroborah Granodiorite|43213|3|Fully described|p57, p68-69, p96, p111, p117, p121-124|Middle Devonian|Middle Devonian|See also p175, p224, p234, p241. Of the largely concealed Taroborah Batholith which has an area of at least 600 km2. Type locality described. Contact metamorphoses basalt in Fork Lagoons beds. Mis-spelt as Taraborah on p87 and p90. K-Ar biotite and hornblende ages respectively. Geochemistry and geophysics detailed. I-type.|372 Ma and 374 Ma (Webb et al., 1963).|||Intrudes Fork Lagoons beds. Is overlain by Silver Hills Volcanics, Reids Dome beds, Aldebaran Sandstone and Red Mountain Formation.|Medium-grained, equigranular to seriate granodiorite with conspicuous larger hornblende crystals; lesser dark grey gabbro and diorite to pink monzonite containing aplite and pegmatite veins. Generally very weathered and lateritised.|
24011|Taroborah Granodiorite|68731|6|Mentioned|p132||||||||Hornblende- and biotite-bearing.|
24011|Taroborah Granodiorite|70856|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey, medium-grained biotite-hornblende granodiorite and tonalite.|
36987|Taromeo Igneous Complex|23799|3|Fully described|p67, p114, p13 Tb. 1|Late Triassic|Late Permian|Formerly Taromeo Tonalite as defined by Murphy et al (1976).  Previously informally known as "Yarraman Granodiorite" and "Taromeo Tonalite" (Gradwell, 1949). Overlain by Main Range Volcanics. Geol. Prov: Yarraman Subprovince (Wandilla Province).||||||
36987|Taromeo Igneous Complex|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
36987|Taromeo Igneous Complex|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||
36987|Taromeo Igneous Complex|60370|5|Briefly described|Map Legend|Triassic|Permian|Granodiorite, tonalite, diorite, gabbro, granite.||||||
36987|Taromeo Igneous Complex|68679|5|Briefly described|p322, p410-411, p413-416|Triassic|Permian|West of the Esk Basin, northern New England Orogen. Comprises multiple, overlapping zoned plutons, each up to 15km in diameter, defined on magnetic images by highly magnetic margins. Intrudes the Yarraman Subprovince. Has lower Na2O and K2O and higher CaO. Geochemical plot. Numerous ages within this range given.|~263 Ma to ~225 Ma.||||Seven phases described in detail on p413. Includes granodiorite, tonalite, diorite, gabbro, granite.|
24514|Taroom Coal Measures|12597|4|Described|p496, p506|||Mimosa Syncline area, Clarence-Moreton Basin. 50-200m thick. Coal deposits and properties described.||Unit in Walloon Coal Measures.|||Lithic and feldspathic labile sandstone interbedded with siltstone, mudstone, carbonaceous shale and coal; local limestone and ironstone lenses.|
24514|Taroom Coal Measures|37991|5|Briefly described|p180|||||||||
24514|Taroom Coal Measures|37993|3|Fully described|p162|||||||||
24514|Taroom Coal Measures|38658|6|Mentioned|p153|||||||||
24514|Taroom Coal Measures|40675|6|Mentioned|Table 9A|||||||||
24514|Taroom Coal Measures|63218|4|Described|pp209-221.     |Middle Jurassic|Middle Jurassic|Surat Basin. Contains three named seams. The article details analyses for coal seam gas.||Unit in Walloon Subgroup.||Overlies Durabilla Formation. Is overlain by Tangalooma Sandstone.||
24514|Taroom Coal Measures|64665|6|Mentioned|p61.|Middle Jurassic|Middle Jurassic|||Unit in Walloon Subgroup.||||
24514|Taroom Coal Measures|64856|5|Briefly described|p87|Middle Jurassic|Middle Jurassic|Of the Walloon Coal Measures (Subgroup) of Jones and Patrick (1979). Middle Jurassic age implied.| | ||||31-JAN-13
24514|Taroom Coal Measures|65003|5|Briefly described|p1-2, p29, p30-32|Middle Jurassic|Early Jurassic|||Of Walloon Subgroup, Surat Basin.|||Incorporates high volatile perhydrous, and bituminous rank coal, with high ash content.|30-MAR-12
24514|Taroom Coal Measures|65096|5|Briefly described|p368-372, p376|Middle Jurassic|Middle Jurassic|Unclear whether this paper is combining Eurombah Formation and Taroom Coal Measures, because the boundary can be difficult to distinguish, or whether Taroom Coal Measures sometimes directly overlies Hutton Sandstone. Up to 130 m thick, coal seams up to 20 m thick. Unit divided into the Auburn, Bulwer and Condamine seams by some workers (e.g. Scott et al., 2004).||Of the Walloon Coal Measures/Walloon Subgroup. ||Overlies the Eurombah Formation. Overlain by the Tangalooma Sandstone.||
24514|Taroom Coal Measures|67133|6|Mentioned|p12-13|||Tends to be kaolinite-rich in Dalby 1 well.||Walloon Subgroup.||||
24514|Taroom Coal Measures|67365|5|Briefly described|p86.|||A number of wells have recently (2009) been completed as CSG producers in this unit, in the Daandine gas field.||||||
24514|Taroom Coal Measures|67402|6|Mentioned|p275|||Surat Basin.||Walloon Subgroup||Overlain by the Juandah Coal Measures.||
24514|Taroom Coal Measures|68117|3|Fully described|p345-353, p354 Fig.9, p355|Middle Jurassic|Middle Jurassic|Jones and Patrick (1981) after Swarbrick (1973)'s intervals 3, 4 and 5 of Injune Creek Group. Redefined by Queensland Gas Company Limited (QGC) as consisting of interval 5 only (intervals 3 and 4 comprise Durabilla Formation). 30-180m thick. The top of this unit is the top of the Auburn Seam or, where that is absent, the base of the first major sandstone interval above the argillaceous interval representing the Auburn Seam. Coal analysis. Gas content vs depth diagram.||Walloon Subgroup.|Auburn, Bulwer (Lower and Upper), Condamine Seams.|Gradationally overlies Durabilla Formation. Is overlain conformably by Tangalooma Sandstone.|Grey to black carbonaceous laminated mudstone with fossil plants; grey and partly micaceous siltstone; light grey, fine, moderately to well sorted sandstone; three coal intervals.|
24514|Taroom Coal Measures|68139|5|Briefly described|p21, 24-25, 28, 30, 32-33|Middle Jurassic|Middle Jurassic|Surat Basin. Maceral composition tabulated, discussed.||Walloon Subgroup.||Overlies Durabilla Formation and Hutton Sandstone. Is overlain by Tangalooma Sandstone.||
24514|Taroom Coal Measures|69574|5|Briefly described|p21-24, 28-32|Middle Jurassic|Middle Jurassic|Surat Basin. Desorbed gas molecular composition and compound-specific isotopes tabulated.||Walloon Subgroup.||Overlies Durabilla Formation. Is overlain by Tangalooma Sandstone.||
24514|Taroom Coal Measures|69594|6|Mentioned|p536|||Jones and Patrick (1981) raised the Walloon Coal  Measures to Subgroup status and included this unit, as well as the Tangalooma Sandstone and Juandah Coal Measures. Scott et al. (2004) separated the basal sandstone unit as the Durabilla Formation. In this study, they are regarded as Members of the Walloon Coal Measures only in the NE Surat Basin.||||||
24514|Taroom Coal Measures|69790|5|Briefly described|p1061, p1065-1078|||Defined by Jones and Patrick (1981). Represents major channel, floodplain and mire deposition in meandering fluvio-lacustrine environments. Thins to the S.  Mined at Commodore and New Acland.||Unit in Walloon Subgroup.||Overlies Durabilla Formation. Is overlain by Tangalooma Sandstone and Juandah Coal Measures.||
24514|Taroom Coal Measures|70374|5|Briefly described|p808, p809 figure 1, p810,811|Oxfordian|Oxfordian|CA-TIMS date from tuff in ~ the middle of the unit in Stratheden 4, eastern Surat Basin.|162.55 +/-0.05 Ma, 162.8 Ma (zircons)|Walloon Coal Measures /Walloon Subgroup.||Overlies Eurombah Formation, Durabilla Formation. Is overlain by Tangalooma Sandstone.|Coal and tuff.|28-SEP-16
24514|Taroom Coal Measures|70628|5|Briefly described|p952,953,957,965 Fig 17|Bajocian|Bajocian|Lower coal layer||Walloon Subgroup|Includes Condamine Sandstone.|Conformably (grades into) overlies Eurombah Formation, Durabilla Formation. Underlies Tangalooma Sandstone.|Minor channel sandstones enveloped in overbank fines and thin, lenticular coal plies; maceral trends indicate an increasingly wet environment during deposition.|
24514|Taroom Coal Measures|70725|5|Briefly described|p11, 13-20, 23-26|Late Jurassic|Late Jurassic|Surat Basin. Formed by water-logged peat overlain by stacked channel sandstones. Maceral composition and vitrinite reflectance graphed and discussed. 13C isotope vs. depth tabulated.||Walloon Subgroup.||Overlies Durabilla and Eurombah Formations. Is overlain by Tangalooma Sandstone.|Thick coal seams, associated with sandstones of variable thickness.|
24514|Taroom Coal Measures|71282|5|Briefly described|p456, p457 Fig.1, p467|||Jones and Patrick (1981). Surat Basin. [The authors of this article incorrectly state that Jones and Patrick "informally" named this unit.]||Walloon Subgroup.||Is overlain by Tangalooma Sandstone.||
24514|Taroom Coal Measures|72297|5|Briefly described|p699, p751|Jurassic|Jurassic|NE Surat Basin. Elsewhere this is part of the Walloon Coal Measures.||Walloon Subgroup.|Condamine, Bulwer Lower, Bulwer Upper, Auburn Seams.|Overlies Durabilla Formation. Is overlain by Tangalooma Sandstone.||
41795|Tartrus Rhyolite|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Lizzie Creek Volcanic Group. Grey, crystal rich rhyolitic ignimbrite.||||||29-SEP-04
41795|Tartrus Rhyolite|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Grey, crystal rich rhyolitic ignimbrite.||||||
41795|Tartrus Rhyolite|61035|4|Described|p8|Early Permian|Late Carboniferous|Of the Lizzie Creek Volcanic Group. Basal unit of the Lizzie Creek Volcanic Group. Geological Province: Connors Sudprovince. Comprises a crystal-rich ignimbrite sheet, several tens meters thick.||||||07-FEB-11
41795|Tartrus Rhyolite|65388|3|Fully described|p112-113; p85, 86, 110, 119, 125, 393|Early Permian|Late Carboniferous|Of Connors Volcanic Group, Connors Arch. Overlies the Leura Volcanics and is overlain conformably by the Mount Benmore Volcanics and Langdale Hill Rhyolite. Weighted mean SHRIMP age: 300.8 +/- 4 Ma. Bluish grey, crystal-rich ignimbrite||||||09-SEP-14
41795|Tartrus Rhyolite|68679|5|Briefly described|p355, p357-358, p362|Cisuralian|Cisuralian|Occurs in the southern Broadsound Range and in the Langdale Inlier, Connors Subprovince. Forms a flat-lying to gently dipping sheet, probably <50m thick. SHRIMP U-Pb zircon age determinations by Fanning et al. (2009).|300.8 +/- 4.1 Ma and 296.9 +/- 3.5 Ma .|Connors Volcanic Group.||Overlies Leura Volcanics. Is overlain by Langdale Hill Rhyolite transgressively (?unconformably), Mount Benmore and Macksford Volcanics.|Crystal-rich rhyolitic ignimbrite.|
41795|Tartrus Rhyolite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Ignimbrite.|
38787|Tawallah Group, Lower|23910|5|Briefly described|p292 Fig. 4|||Informal name - see Tawallah Group.||||||04-MAR-20
38787|Tawallah Group, Lower|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Sandstone. Geological Province: Southern McArthur Basin.||||||
38787|Tawallah Group, Lower|60483|5|Briefly described|p27, p64|||Informal - see Tawallah Group. Discusses low reflectivity.||||||
38787|Tawallah Group, Lower|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||includes Yiyintyi Sandstone to McDermott Formation..||Quartzose sandstone; subordinate conglomerate, ferruginous sandstone, dolostone, mudstone; basaltic volcanics; dolerite sills and dykes.|04-MAR-20
38787|Tawallah Group, Lower|73412|6|Mentioned|p18|||Southern McArthur Basin. Deposition during N-S to NE-SW directed extension.|c.1760-1740 Ma.|||||
80476|Tea Tree Granite|64250|6|Mentioned|p11 fig 3|Calymmian|Calymmian|[???Shown as part of the Kalkadoon-Leichhardt Belt of QLD]|1512 +/- 5 Ma|||||
80476|Tea Tree Granite|65396|6|Mentioned|p7, p82, p84, p157, p175, p241|Calymmian|Calymmian|Kalkadoon-Leichhardt Belt, Mount Isa Inlier. Associated with the Isan Orogeny. Appears as Tea tree Granite on p157.|1512 +/- 5 Ma|||||
80476|Tea Tree Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1512 +/- 5 Ma|||||
24018|Tea Tree Granodiorite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
24018|Tea Tree Granodiorite|22781|4|Described|p27|Paleozoic|Paleozoic|Flyspeck Supersuite||||||07-NOV-08
24018|Tea Tree Granodiorite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intruded by Kintore and Ebagoola Granites.||||||
24018|Tea Tree Granodiorite|42610|3|Fully described|p25|Early Devonian|Early Devonian|Age ass. same as Glen Garland Granodiorite, 398Ma. Prev. incl. in Flyspeck Granodiorite & "Kintore A||||||
24018|Tea Tree Granodiorite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
24018|Tea Tree Granodiorite|71849|6|Mentioned|p120|||Significance of allanite-epidote association discussed.||Flyspeck Supersuite.||||
78958|Tecoma Granodiorite|65388|2|Defined|p332-333, p237, 238, 295, 303, 304, 327|Early Triassic|Early Permian|Of Coonambula Suite. Previously Tecoma Granite. Variation on name for same three samples with geochemical affinities to early Permian Coonambula Suite rocks. Enclosed by Colodon Granodiorite. Relationships uncertain. Age not known. May be either Early Permian or Late Permian to Early Triassic. Two 'Colodon Granodiorite samples' also plot with Tecoma Granodiorite and Coonambula Suite rocks. Two other samples plot within Tandora and Wingfield Suites, so unit may be composite. Light grey, fine-grained granite to granodiorite. See also p338, 339-340.||||||
78958|Tecoma Granodiorite|68679|5|Briefly described|p417, p419|||Northern part of the Rawbelle Batholith. ~22 km2 as two bodies. Geochemistry suggests unit may be composite and includes early Permian components; analyses plot with Coonambula, Tandora and Wingfield Suites.||||Is enclosed by Colodon Granodiorite (may be older rafts).|Hornblende-biotite granodiorite; common leucocratic dykes.|
69502|Teddys Creek Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, even-grained biotite granite.|
69502|Teddys Creek Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||White to pink, medium-grained, even-grained biotite granite.|
35191|Teemburra Igneous Complex|23042|4|Described|p94,5,6, Fig 2|Early Permian|Carboniferous|||||||
35191|Teemburra Igneous Complex|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35191|Teemburra Igneous Complex|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Grey to pink, fine-grained biotite granite and leucogranite; grey, medium- to coarse-grained biotite-hornblende granodiorite with mafic xenoliths; coarse- to very coarse-grained hornblende diorite or gabbro; magma-mingled fine-grained diorite and dolerite||||||
35191|Teemburra Igneous Complex|65388|2|Defined|p386-388, 135, 362, 364, 365, 380, 389|Early Permian|Early Permian|Northern Connors Arch. Southern Urannah Batholith. May intrude Pisgah Igneous Complex. Probably intruded by Yarravale Creek Granite, and maybe by Uruba Granite. K-Ar dating of biotite and hornblende yielded recalculated minimum ages of 273Ma and 284Ma respectively (Webb & McDougall, 1968). 3 bodies mapped. Range of rocks includes equigranular to moderately porphyritic biotite granite and granodiorite and a net-veined complex of hornblende diorite and hornblende-biotite granodiorite.||||||
25522|Teewah Sands|37203|6|Mentioned|p61|||||||||
25522|Teewah Sands|44662|2|Defined|Fig.56,p406,407|||||||||
25522|Teewah Sands|44663|14|Not recorded|p122|||||||||
25522|Teewah Sands|44754|14|Not recorded|p7,map||Quaternary|||||||
25522|Teewah Sands|44783|14|Not recorded|p2|||||||||
25522|Teewah Sands|45025|6|Mentioned|p116|||||||||
25522|Teewah Sands|45440|14|Not recorded|p.47|||||||||
26167|Telegraph Creek Member|39493|2|Defined|p95|late Eocene|middle Eocene|Mid to late Eocene||||||
26167|Telegraph Creek Member|40116|6|Mentioned|p29|||||||||
26167|Telegraph Creek Member|41927|5|Briefly described|p64|||||||||
26167|Telegraph Creek Member|42021|5|Briefly described|p321|||||||||
26167|Telegraph Creek Member|71092|6|Mentioned|p232|Eocene|Eocene|Middle-late Eocene; contains the oldest meiolaniid turtle remains in Australia.||Rundle Formation.|||Has a marker oil shale bed.|
26167|Telegraph Creek Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
35037|Telemark Granodiorite|23037|4|Described|p94||Triassic|Intrudes Culcraigie Granite.||||||
35037|Telemark Granodiorite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Grey, medium-grained hornblende granodiorite.||||||
35037|Telemark Granodiorite|65388|2|Defined|p333-334, 301, 303, 304, 327, 332, 340|Triassic|Triassic|New name. Of Tandora Suite. Previously included in Culcraigie Granite. Distinguished by magnetics. Interpreted as intruding Tandora Granodiorite, Culcraigie Granite. K-Ar (hornblende) age 226 Ma from sample that is probably Telemark Granodiorite. Hence probable age given. Dominant rock type comprises grey, medium to coarse-grained granodiorite. ||||||
35037|Telemark Granodiorite|68679|5|Briefly described|p418-420|||An ovoid, ~20 km2 pluton in the Rawbelle Batholith. Geochemistry plot.|226 +/- 7 Ma (K-Ar: Whitaker et al., 1974).|Tandora Suite.||Intrudes Culcraigie Granite.|Hornblende granodiorite; magnetic images show strong annular anomaly (4.5km across) with less magnetic core possibly representing a more extensive subsurface diorite phase.|
32858|Templeton Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event..||Sybella Suite|||Foliated coarse-grained porphyritic biotite granite.|
32858|Templeton Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Foliated coarse-grained porphyritic biotite granite.|
41101|Ten Mile Granite|50301|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
41101|Ten Mile Granite|65388|4|Described|p276-277, p236 Fig. 81, p256|Early Permian|Late Carboniferous|Tentatively interpreted to post-date the Glen View Quartz Monzodiorite and Wind Mill Diorite. Age uncertain. Pale grey, leucocratic hornblende-biotite monzogranite.||||||
41101|Ten Mile Granite|68679|5|Briefly described|p407-408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Age relationships with two other intrusives given.|||||Pale grey, leucocratic, hornblende-biotite monzogranite.|
26168|Teningie Creek Member|39493|2|Defined|p98|late Eocene|middle Eocene|Mid to late Eocene||||||
26168|Teningie Creek Member|40116|6|Mentioned|p29|||||||||
26168|Teningie Creek Member|41927|5|Briefly described|p64|||||||||
26168|Teningie Creek Member|42021|6|Mentioned|Fig.3 P320|||||||||
26168|Teningie Creek Member|71092|6|Mentioned|p232|Eocene|Eocene|||Rundle Formation.||||
26168|Teningie Creek Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
27967|Tennyson Volcanic Subgroup|23423|4|Described|p306 Table 7.3||Late Carboniferous|Intruded by Lags Microgranite, and Petford Granite. Featherbed Volcanic Group. Overlying unit Fisherman Rhyolite; Underlying unit Hodgkinson Formation, Boonmoo Volcanic Subgroup.||||||
27967|Tennyson Volcanic Subgroup|23501|6|Mentioned|map legend|Late Carboniferous|Late Carboniferous|Of Featherbed Volcanic Group.||||||
27967|Tennyson Volcanic Subgroup|23616|5|Briefly described|Table 3 p48||Late Carboniferous|Unconform. on Hodgkinson Fm rocks; also overlies Boonmoo Volcanic Subgp in places; o'lain locally by Fisherman Rhyolite; intruded by Lags Microgranite, Petford Granite, rare rhyolite dykes and plug of olivine basalt (Cainozoic). Of Featherbed Volcanic Group.||||||02-APR-15
27967|Tennyson Volcanic Subgroup|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Featherbed Volcanic Group.||||||15-JUN-06
27967|Tennyson Volcanic Subgroup|43626|4|Described|p10,30||Late Carboniferous|||||||
27967|Tennyson Volcanic Subgroup|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
27967|Tennyson Volcanic Subgroup|60425|4|Described|p46 Tb. 3|Late Carboniferous|Late Carboniferous|Of Featherbed Volc. Group.Contains Lappa + Allsorts Rhyolites (+3informal subunits) + Dalnotter Dacite.Thickness: ~430m.Unconformable on Hodgkinson Fm; also over Boonmoo Volc.Subgp in places; locally under Fisherman Rhyolite. Detailed lithology provided.||||||07-FEB-11
27967|Tennyson Volcanic Subgroup|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Featherbed Volcanic Group.|Includes Dalnotter Dacite; Allsorts and Lappa Rhyolites.|||
27967|Tennyson Volcanic Subgroup|68576|5|Briefly described|Q_11: p12-13|||Petford area.|||||Includes rhyolitic ignimbrite with variable amounts of lithic and crystal fragments.|
27967|Tennyson Volcanic Subgroup|69593|5|Briefly described|p485|Late Carboniferous|Late Carboniferous|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.||||
40574|Term Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Stretton Sandstone and Looking Glass Formation.|||
40574|Term Supersequence|63866|5|Briefly described|p53, p56|||Isa Superbasin.|||Includes the Stretton Sandstone.|||
40574|Term Supersequence|65228|5|Briefly described|p32, pp35-37, Figs.22-23, 28.|Statherian|Statherian|Up to 2,500 m thick. Represented by basal Stretton Sandstone and Looking Glass Sandstone (in McArthur River Region), and by Termite Range Formation and lower part of Lawn Hill Formation (in southern Lawn Hill Platform). Gamma ray log, lithology and facies detailed.|c.1630-1620 Ma.|||Overlies River Supersequence.|Turbiditic and hemipelagic sandstones and shales.|
40574|Term Supersequence|66843|6|Mentioned|p38 Fig.10|||Said to be "informally" named.||||||
40574|Term Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40574|Term Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier.|~1635-1615 Ma.|McNamara Group.||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation and Termite Range Formation.||||||
40574|Term Supersequence|69056|6|Mentioned|p56|||||||||
40574|Term Supersequence|69591|5|Briefly described|p27, p43, p46-47, p54, p108|||Mount Isa Province. Deeper-water medium- to coarse-grained clastic turbidite packages. Recognised in the Nathan Group (NT). Consists of the Termite Range Formation.||||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|70897|5|Briefly described|p39, Fig.1.7.1-3,7|||Shows rapid thickness and lithofacies variations across regional fault systems.||||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation and uppermost Termite Range Formation.|||||White and grey thick-bedded sandstone and lithic sandstone interbedded with siltstone.|
40574|Term Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||||Fissile to flaggy tuff and tuffaceous siltstone, thinly interbedded micaceous siltstone, shale and claystone. Grey to black carbonaceous shale containing light grey silty carbonate concretions and flaggy siltstone interbeds, minor tuff.|
40574|Term Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Paleoproterozic|Paleoproterozic|This unit requires more Rock-Eval for hydrocarbon potential to be determined.||||Overlies River Supersequence and underlies Lawn Supersequence.||
40574|Term Supersequence|73144|4|Described|p8-9, p11-12, p20, p25|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains five third order sequences [see article for more detail on third order sequences]. Deposited in mid-outer self, silty turbidites and submarine fans (Krassay et al., 2000). Forms a series of onlapping wedges which gradually thin to the north. An emergent basement high associated with the Murphy Inlier is considered as the source of turbidites. Capped by a significant erosional event.|1615-1630 Ma|||Includes a portion of the Lawn Hill Formation, and Termite Range Formation.|Siltstone, shale, carbonaceous siltstone, sandstone including coarse-grained sandy turbidites.|
28031|Terrible Creek Granite|23420|5|Briefly described|p 152 table 4.8||Early Devonian|In the Fish Creek Suite of the Kintore Supersuite||||||
28031|Terrible Creek Granite|23496|5|Briefly described|Table 2, p42|Devonian|Silurian|of Fish Creek Suite, Kintore Supersuite.||||||
28031|Terrible Creek Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Fish Creek Suite.||||||
28031|Terrible Creek Granite|43596|4|Described|p33,  p28 Tb. 3|||Unassigned S-type. White to pale grey, med.-gr. garnet-biotite-muscovite granite with scattered sparse muscovite phenocrysts. Contains rare enclaves of Aralba Granite up to several metres across; granites are similar suggesting simultaneous emplacement.||||||27-JAN-09
28031|Terrible Creek Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
80780|Terry Creek Quartz Monzodiorite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Grey, medium-grained, uneven-grained biotite-hornblende quartz monzodiorite; with minor titanite and traces of clinopyroxene; extensively deformed with a well-developed gneissic foliation in places.|
25525|Tewinga Group|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Includes: Argylla Formation.||||||
25525|Tewinga Group|22461|5|Briefly described|Fig 1 p464|||||||||
25525|Tewinga Group|23069|5|Briefly described|p775 (fig 1)|||||||||
25525|Tewinga Group|23518|4|Described|p9 Fig. 3|Proterozoic|Proterozoic|Geological Province: Kalkadoon-Ewen Province.||||||
25525|Tewinga Group|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Overlain by the Mary Kathleen Group||||||
25525|Tewinga Group|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25525|Tewinga Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Overlies the Magna Lynn Metabasalt.||||||25-AUG-04
25525|Tewinga Group|30530|6|Mentioned|p515|||Also mentioned p516.||||||15-MAR-18
25525|Tewinga Group|30531|6|Mentioned|p15|||Also mention p18 and p22.||||||15-MAR-18
25525|Tewinga Group|30532|6|Mentioned|p113|||||||||
25525|Tewinga Group|30534|6|Mentioned|p300|||||||||
25525|Tewinga Group|30535|6|Mentioned|p403|||||||||
25525|Tewinga Group|30536|2|Defined|p102|Carpentarian|Carpentarian|||||||
25525|Tewinga Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25525|Tewinga Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25525|Tewinga Group|32660|4|Described|Table 5|||||||||
25525|Tewinga Group|32959|6|Mentioned|p31|||||||||
25525|Tewinga Group|33111|6|Mentioned|p5|||||||||
25525|Tewinga Group|33900|4|Described|p7|||Mentioned p4.||||||15-MAR-18
25525|Tewinga Group|35074|6|Mentioned|p206|||See also Fig.2 and geochemistry P213.||||||
25525|Tewinga Group|35114|6|Mentioned|p203|||||||||
25525|Tewinga Group|35286|6|Mentioned|p143|||||||||
25525|Tewinga Group|35295|6|Mentioned|p603|||||||||
25525|Tewinga Group|35369|6|Mentioned|PB5|||||||||
25525|Tewinga Group|35495|6|Mentioned|p349|||||||||
25525|Tewinga Group|36052|4|Described|p419|||See also Fig.2.||||||
25525|Tewinga Group|36226|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Carpentarian to Lower Proterozoic||||||07-NOV-08
25525|Tewinga Group|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
25525|Tewinga Group|37217|6|Mentioned|p655|||||||||
25525|Tewinga Group|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25525|Tewinga Group|37462|4|Described|Table4.VII|||||||||
25525|Tewinga Group|37565|6|Mentioned|Fig.5|||||||||
25525|Tewinga Group|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25525|Tewinga Group|37862|6|Mentioned|p581|||||||||
25525|Tewinga Group|38234|4|Described|p100|||||||||
25525|Tewinga Group|38275|6|Mentioned|p181|||||||||
25525|Tewinga Group|38276|6|Mentioned|Fig.1|||||||||
25525|Tewinga Group|38278|6|Mentioned|Fig.1|||||||||
25525|Tewinga Group|38350|4|Described|p5|||||||||
25525|Tewinga Group|38448|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
25525|Tewinga Group|38560|6|Mentioned|p114|||||||||
25525|Tewinga Group|38900|6|Mentioned|Fig.2|||||||||
25525|Tewinga Group|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Argylla Formation.  Overlain by the Malbon Group.||||||25-AUG-04
25525|Tewinga Group|39202|6|Mentioned|p228|||||||||
25525|Tewinga Group|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25525|Tewinga Group|39445|5|Briefly described|p39|||Leichhardt Block. See also Table 2||||||
25525|Tewinga Group|39496|6|Mentioned|p5|||||||||
25525|Tewinga Group|39556|5|Briefly described|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic to Carpentarian||||||07-NOV-08
25525|Tewinga Group|39602|6|Mentioned|p633|||||||||
25525|Tewinga Group|39622|6|Mentioned|p19|||See also Appendix||||||
25525|Tewinga Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle Proterozoic||||||07-NOV-08
25525|Tewinga Group|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25525|Tewinga Group|39937|6|Mentioned|Fig.1|||||||||
25525|Tewinga Group|40221|6|Mentioned|p22|||||||||
25525|Tewinga Group|40623|5|Briefly described|p95|||||||||
25525|Tewinga Group|40648|6|Mentioned|p4|||||||||
25525|Tewinga Group|40840|6|Mentioned|Map legend|||||||||
25525|Tewinga Group|40984|4|Described|p389|||||||||
25525|Tewinga Group|41125|6|Mentioned|p45|||||||||
25525|Tewinga Group|41306|4|Described|p5|||||||||
25525|Tewinga Group|41307|4|Described|p5|||||||||
25525|Tewinga Group|41319|6|Mentioned|p205|||||||||
25525|Tewinga Group|41464|6|Mentioned|Map legend|Proterozoic||||||||
25525|Tewinga Group|41556|6|Mentioned|Map legend|Proterozoic||||||||
25525|Tewinga Group|41568|4|Described|p5|||||||||
25525|Tewinga Group|41744|6|Mentioned|p406|||||||||
25525|Tewinga Group|41791|6|Mentioned|p247|||||||||
25525|Tewinga Group|41978|6|Mentioned|p493|||||||||
25525|Tewinga Group|42201|6|Mentioned|p292|||||||||
25525|Tewinga Group|43595|5|Briefly described|p439|||||||||
25525|Tewinga Group|43620|6|Mentioned|Fig.1,p51|||||||||
25525|Tewinga Group|45136|4|Described|Table 1|||||||||
25525|Tewinga Group|45161|4|Described|p16|||See also p39.||||||15-MAR-18
25525|Tewinga Group|45166|4|Described|p12|||||||||
25525|Tewinga Group|46801|6|Mentioned|Fig. 14|||||||||
25525|Tewinga Group|46859|6|Mentioned|p311|||||||||
25525|Tewinga Group|46919|6|Mentioned|p219|||See also p213.||||||15-MAR-18
25525|Tewinga Group|46960|6|Mentioned|p220|||||||||
25525|Tewinga Group|46962|4|Described|Table 1|||See also Fig.3.||||||
25525|Tewinga Group|46995|6|Mentioned|p267|||||||||
25525|Tewinga Group|46996|6|Mentioned|p273|||||||||
25525|Tewinga Group|49009|6|Mentioned|p7|||||||||
25525|Tewinga Group|49041|5|Briefly described|Table 2|||See also Table 3. Mention Table 4||||||
25525|Tewinga Group|50536|6|Mentioned|p2.2|||Intruded by Kalkadoon Supersuite.||||||
25525|Tewinga Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Leichhardt Volcanics, Magna Lynn Metabasalt, Argylla Formation.||||||
25525|Tewinga Group|61922|6|Mentioned|p11|||Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
25525|Tewinga Group|63023|6|Mentioned|p1024 Fig. 1|||||||||
25525|Tewinga Group|64248|6|Mentioned|p32, p33 Fig.1, p40 Fig.6, p41 Tb. 2 |||See also p43 Fig.11. Eastern Succession, Mount Isa.||||||
25525|Tewinga Group|64250|5|Briefly described|p8, p10 fig 2, p13 figs 4,5, p14, p15||||||Includes Argylla Formation.|Unconformably overlies Plum Mountain Gneiss. Is overlain by Marraba Volcanics.||
25525|Tewinga Group|65396|6|Mentioned|p4, p17 Fig.9, p23, p171, p173, p178-179|||See also p182-183, p199, p213, p222, p234-241, p266-267, p272. Cover Sequence 2, Eastern Succession, Mount isa Inlier. Appears as Tewinga group on p266-267.|||Includes Argylla Formation|Overlain by Ballara Quartzite, Marraba Volcanics, Mitakoodi Quartzite.||
25525|Tewinga Group|67323|6|Mentioned|p71-72|Paleoproterozoic|Paleoproterozoic|Associated with clusters of Au anomalies to the NE of Duchess, and Cu and minor IOGC anomalies.||||||
25525|Tewinga Group|67539|6|Mentioned|p6|||Duchess-Dajarra area. Intensely foliated quartzofeldspathic gneiss and subordinate mafic gneiss were previously mapped as undivided Tewinga Group gneiss.|||||Dominated by intensely foliated quartzofeldspathic gneiss and subordinate mafic gneiss.|
25525|Tewinga Group|68146|5|Briefly described|p57, p193-194|||Southern Mount Isa Region. An area 15km NE of Dajarra, which was previously mapped as undivided Tewinga Group, is here included in Kalkadoon Granodiorite.||||||02-NOV-18
25525|Tewinga Group|68575|6|Mentioned|p124|||Part of this unit (labelled Pet) in the Dajarra 1:100 000 sheet is now the Paper Tank Microgranite.||||||
25525|Tewinga Group|69222|6|Mentioned|p221|Paleoproterozoic|Paleoproterozoic|Metamorphosed during the 1890-1840 Ma Barramundi Orogeny.||||||
25525|Tewinga Group|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1855+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss, granodiorite.|
25525|Tewinga Group|73137|5|Briefly described|p21||||||Argylla Formation at top.|Unconformably overlain by Mary Kathleen Group.||07-OCT-22
25525|Tewinga Group|73553|5|Briefly described|p21, p250|||Of Derrick et al., (1977a).|||Leichhardt Volcanics, Magna Lynn Metabasalt, Argylla Formation|||
36527|The Cornishman rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 182.||||||
36651|The Falls Granite|23420|5|Briefly described|p 152 table 4.8||Early Devonian|Intrudes Lukinville Granodiorite. Kintore Supersuite.||||||
36651|The Falls Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
27302|The Fisheries Basalt|23497|5|Briefly described|Table 1|Pleistocene|Pliocene|Of Atherton Subprovince. of Willmott and others, 1988. Age: K-Ar 2.2Ma. Thickness ~50m.||||||03-JUN-09
27302|The Fisheries Basalt|23507|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
27302|The Fisheries Basalt|42625|5|Briefly described|Map legend|Pleistocene|Pliocene|Reserved.||||||
27302|The Fisheries Basalt|42810|2|Defined|Table 1 P14|Pleistocene|Pliocene|see also p30.||||||20-AUG-08
27302|The Fisheries Basalt|60425|6|Mentioned|p42 Tb. 3|Miocene|Miocene|Part of Atherton Basalt grouping.||||||07-FEB-11
36239|The Gorge Rhyolite|23423|5|Briefly described|p309 Table 7.3||Late Carboniferous|Claret Creek Volcanics||||||
36239|The Gorge Rhyolite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Claret Creek Ring Complex, Claret Creek Supersuite.||||||
36239|The Gorge Rhyolite|23624|5|Briefly described|p26|Late Carboniferous|Late Carboniferous|Formerly included in the Elizabeth Creek Magma Series (Bailey 1977). Part of Claret Creek Supersuite.||||||05-JAN-05
36239|The Gorge Rhyolite|60425|4|Described|p50 Tb. 3, p284-5 Appdx. |Late Carboniferous|Late Carboniferous|Of Claret Creek Volcanics (Claret Creek Supersuite, p50); also assigned to Lappa Suite (O'Briens Creek Supersuite, p284-5). Age: ~302Ma and 300+/-6Ma (Rb-Sr). Welded rhyolitic ignimbrite - more detailed lithology included; I-type.||||||07-FEB-11
36239|The Gorge Rhyolite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Undivided porphyritic microgranite, flow-banded rhyolite, dacite?, intrusive rhyolitic to dacitic? breccia.|
36239|The Gorge Rhyolite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Undivided porphyritic microgranite, flow-banded rhyolite, dacite?, intrusive rhyolitic to dacitic? breccia.|
24024|The Maze Granite|22847|3|Fully described|p 40|||||||||
24024|The Maze Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
24024|The Maze Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 111. Assumed to be I-Type.||||||
24024|The Maze Granite|42245|2|Defined|p30|Ordovician||||||||
24024|The Maze Granite|43093|4|Described|Appendix 1||Ordovician|||||||
24024|The Maze Granite|43259|4|Described|Appendix 1,p23.||Ordovician|||||||
24024|The Maze Granite|43933|5|Briefly described|Map Legend||Ordovician|||||||
24024|The Maze Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
76892|The Monument Syenite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Cream, medium- to locally coarse-grained, equigranular to locally porphyritic, moderately to poorly foliated, biotite-hornblende syenite; commonly exhibits good linear fabric.|
76892|The Monument Syenite|69591|5|Briefly described|p60|||Mount Isa Province.|||||Cream, medium-grained to locally coarse-grained, equigranular to locally porphyritic, moderately to poorly foliated biotite-hornblende syenite; strong linear fabric.|
76892|The Monument Syenite|73553|5|Briefly described|p2, p20, p45, p47 Fig.3.6.1,|||Mary Kathleen Domain. Tentatively assigned to Argylla Igneous Province. Included in Kalkadoon Granite by Carter and Opik (1963), delineated and described as a subunit of Corella Formation by Blake et al., (1982a), also described by Hutton and Withnall, (2013). Delineated as a discrete intrusive unit during 2006-2009 GSQ-GA mapping, interpreted as emplaced during the 'Wonga/Burstall Igneous Event'. Very little outcrop. Reddish tones on radiometric images. Variable low-moderate aeromagnetic responses. Mineralogically and chemically distinct from other intrusive units in the domain. Unit is cut by a deformed pegmatite emplaced at ~1775 Ma (U-Pb zircon LA-ICP-MS). See also p49-50, p53-58, p258.||||Enclosed by and reportedly intrudes Corella Formation|Heterogeneous, recrystallised meta-igneous unit. Grey-dark grey, fine-grained (arfvedsonite?-) biotite to arfvedsonite?-nepheline syenite. Very strong linear fabric and gneissic banding.|03-FEB-23
38895|The Narrows Group|24420|4|Described|p9|Eocene|Eocene|Includes the Worthington, Rundle and Curlew Formations.||||||
38895|The Narrows Group|50207|5|Briefly described|Map Legend|Tertiary|Tertiary|Includes: Curlew Formation, Rundle Formation, Worthington Formation.||||||
38895|The Narrows Group|68008|3|Fully described|p271-273|Eocene||Originally the Casuarina-Narrows Series of Dunstan (1913), for the Tertiary sediments of The Narrows Graben. Renamed The Narrows Beds by Kirkegaard et al. (1970). Subdivided into three units by Henstridge and Missen (1982). Referred to as often as not in this study as The Narrows beds [?] (p275, p281, p291). The type section is a composite section, based on core from two boreholes: GSQ Rockhampton 2 and Southern Pacific Petroleum's RD66. Over 1000m thick. Age from fossil assemblages. Intruded by 26.8 Ma dolerite. Age given as Tertiary.|||Curlew, Rundle Formations and Worthington formation.|Abuts [presumably overlies] Wandilla and Doonside Formations. Is correlated (tentatively) with lower part of Casuarina beds.||
41108|The Pride Gabbro|50301|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
41108|The Pride Gabbro|65388|2|Defined|p334, p301 Fig 98, 327|Early Triassic|Late Permian|New name? Intrudes the late Permian Barfield Formation of the Back Creek Group. Rocks along contact indurated and hornfelsed. Mainly dark grey, medium-grained, slightly to moderately porphyritic gabbro. ||||||
41108|The Pride Gabbro|68679|5|Briefly described|p419|||An elongate, ~1 km2 pluton west of the main Rawbelle Batholith.||||Intrudes Barfield Formation (Back Creek Group).|Olivine-clinopyroxene gabbro (locally layered).|
68989|The Shacks Mylonite|65388|6|Mentioned|p70 Fig. 28|||Wandilla Subprovince, northern Yarrol Province.||||||
68989|The Shacks Mylonite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Broome Head, Duckpond Road and Gaythorn Metamorphics, Sabina Point Schist, Townshend Formation, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
68989|The Shacks Mylonite|68679|6|Mentioned|p308, p312-313, p347|Carboniferous|Late Devonian|Wandilla Subprovince, Northern Yarrol Province.||||||
68989|The Shacks Mylonite|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
75664|The Three Brothers Gabbro|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Medium to dark grey, medium to locally fine-grained, uneven-grained to locally porphyritic hypersthene-augite gabbro; with minor quartz, biotite, and hornblende in varying proportions; locally foliated to gneissic; minor coarse hornblendite.|
22984|Theodolite Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
22984|Theodolite Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
22984|Theodolite Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
22984|Theodolite Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V127. I-Type.||||||
22984|Theodolite Rhyolite|23616|5|Briefly described|Table 3 p48|||Of Boonmoo Volcanic Subgroup||||||
22984|Theodolite Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
22984|Theodolite Rhyolite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|of Boonmoo Volcanic Subgroup.||||||
22984|Theodolite Rhyolite|43626|2|Defined|p28||Late Carboniferous|between 306+/-3 Ma and 304+/-4 Ma||||||
22984|Theodolite Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
22984|Theodolite Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group). Detailed lithology for Boonmoo Subgroup included.||||||07-FEB-11
22984|Theodolite Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Boonmoo Volcanic Subgroup.|||Cream to grey, rhyolitic fine-ash vitric to coarse-ash crystal tuff, quartzose, sandy and pebbly siltstones, pebble conglomerate; medium-dark grey, intensely welded, lithics-poor to lithics-rich, crystal-rich, hornblende-biotite rhyolitic ignimbrite.|
42392|Theodolite Siltstone|60281|5|Briefly described|Fig. 33 App 1|Cretaceous|Cretaceous|Of the Maryborough Formation.  Geological Province: Maryborough Basin.||||||
27911|Theresa Creek Volcanics|22543|6|Mentioned|p63||Middle Devonian|assigned to Anakie Province||||||
27911|Theresa Creek Volcanics|22557|6|Mentioned|p569|||||||||
27911|Theresa Creek Volcanics|22604|5|Briefly described|p443, Fig.1 p438||Devonian|Middle? Devonian||||||
27911|Theresa Creek Volcanics|22800|5|Briefly described|Fig.14 p592|Frasnian|Frasnian|||||||
27911|Theresa Creek Volcanics|23522|5|Briefly described|p250 Fig 6|Early Carboniferous|Late Devonian|||||||
27911|Theresa Creek Volcanics|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
27911|Theresa Creek Volcanics|31999|6|Mentioned|p135|||Table 1||||||
27911|Theresa Creek Volcanics|32493|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
27911|Theresa Creek Volcanics|34389|4|Described|Table 1|||Middle Devonian||||||
27911|Theresa Creek Volcanics|34408|6|Mentioned|p185|||On table||||||
27911|Theresa Creek Volcanics|38527|6|Mentioned|p306|||||||||
27911|Theresa Creek Volcanics|39445|5|Briefly described|Table 5|||See also P73||||||
27911|Theresa Creek Volcanics|41246|6|Mentioned|Map legend|Devonian||||||||
27911|Theresa Creek Volcanics|42614|6|Mentioned|Table 2 P10|||||||||
27911|Theresa Creek Volcanics|42747|5|Briefly described|p36, Fig.10|||see also Fig.2||||||
27911|Theresa Creek Volcanics|43029|5|Briefly described|Fig.1,p13|||||||||
27911|Theresa Creek Volcanics|43204|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Anakie Inlier||||underlies Silver Hills Volcanics||23-DEC-11
27911|Theresa Creek Volcanics|43213|2|Defined|p9, p17, p19, p21, p67, p69-71, p117|Devonian|Devonian|See also p125-129, p190, p229-230, p237, p240, p245. Veevers et al. (1964), Olgers et al. (1967). Type area described. Unfossiliferous: exact age is uncertain, but is intruded by possibly comagmatic 370-380 Ma granitoids of the Retreat Batholith. Abbreviated to Theresa Volcanics on p19. Regarded as part of Drummond Basin basement. Has lithological and stratigraphic similarities with Dunstable Volcanics in the Nogoa Anticline. Hosts the Consols Cu prospect. Geophysics and chemical analyses detailed.||||Unconformably overlies Bathampton Metamorphics. Probably age-equivalent to Capella Creek beds. Is intruded by Iron Hut Quartz Monzonite. Is overlain unconformably by Silver Hills Volcanics.|Basaltic to andesitic lava, grey, aphyric to porphyritic and magnetic; volcaniclastic rocks: breccias and conglomerates, grey to green, angular to rounded matrix-supported clasts, poorly to moderately sorted; rare tuff and volcanilithic arenite.|
27911|Theresa Creek Volcanics|43461|14|Not recorded|p616,Table p618||Frasnian|Probably equivalent to Silver Hills Volcanics||||||
27911|Theresa Creek Volcanics|43861|5|Briefly described|25, 28||Devonian|Unconformably overlies Anakie Metamorphic Group||||||
27911|Theresa Creek Volcanics|43994|14|Not recorded|Map Legend|||||||||
27911|Theresa Creek Volcanics|43998|4|Described|p20,map|Carboniferous|Devonian|||||||
27911|Theresa Creek Volcanics|43999|14|Not recorded|p95,96||Late Devonian|||||||
27911|Theresa Creek Volcanics|44331|14|Not recorded|Map Legend||Late Devonian|||||||
27911|Theresa Creek Volcanics|44337|5|Briefly described|Map Legend||Late Devonian|Lithology.||||||
27911|Theresa Creek Volcanics|45071|3|Fully described|p19|||On Table 1||||||
27911|Theresa Creek Volcanics|45073|6|Mentioned|p14|||Refers Veerers et al. (1964a)||||||
27911|Theresa Creek Volcanics|48843|2|Defined|p.8,10,17-19; map|Late Devonian|Middle Devonian|||||||
27911|Theresa Creek Volcanics|48845|14|Not recorded|p9,10|||||||||
27911|Theresa Creek Volcanics|65214|6|Mentioned|p282|Devonian|Devonian|NSW, Telemon. Appears in text as Theresa Ck Volcanics. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
27911|Theresa Creek Volcanics|67028|6|Mentioned|p372 Tb. 5|Silurian|Ordovician|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|428-488 Ma magnetic age range|||||10-AUG-15
27911|Theresa Creek Volcanics|68412|5|Briefly described|Map legend|||Age max: Middle Devonian? Age min: Middle Devonian?|||||Aphyric to porphyritic andesite to trachyandesite lava, volcaniclastic arenite and breccia.|23-JUN-15
27911|Theresa Creek Volcanics|68553|6|Mentioned|Map legend|Devonian|Devonian|This unit, as well as the Ukalunda and Sedgeford Formations, the Douglas Creek Limestone, the Dunstable Volcanics, and unnamed Devonian sedimentary and volcanic units, are all mapped under the symbol, Da.||||||
27911|Theresa Creek Volcanics|68731|5|Briefly described|p120, p151 Fig 3.51, p172|Devonian|Devonian|~ 15 km southwest of Clermont. Withnall et al. (1995). Exposure is relatively poor and the succession is considered to have formed in a subaerial environment as fossils are absent. Age determination discussed in detail.||||Unconformably underlain by the Anakie Metamorphic Group.|Comprises mainly mafic lavas with lesser breccia and conglomerate and rare tuff and volcaniclastic sandstone.|
27911|Theresa Creek Volcanics|68900|6|Mentioned|p4|Devonian|Devonian|Drummond Basin.||||||
27911|Theresa Creek Volcanics|69952|5|Briefly described|p2 Tb.i, p6, p115-119|Late Devonian|Middle Devonian|South of Clermont; Anakie Province. SHRIMP U-Pb zircon reconnaissance maximum depositional age supports previous interpretations that this unit is coeval, and possibly comagmatic, with granitoids of the Retreat Batholith. It also refutes a proposed (Anderson et al., 2004) Ordovician age for the unit, based on a suggested correlation with Fork Lagoons beds.|382 +/- 7 Ma (Cross et al., 2015).|||Unconformably overlies Anakie Metamorphic Group. Is intruded by Iron Hut Quartz Monzonite.|Mostly mafic volcanics (basalt to andesite), lesser breccia, conglomerate, rare tuff and volcaniclastic arenite.|
27911|Theresa Creek Volcanics|70033|5|Briefly described|p1, p13|||In southern Anakie Province.|~382 Ma, Cross et al. 2015|||||
27911|Theresa Creek Volcanics|71592|5|Briefly described|Appendix A.|||Anakie Province, Thomson Orogen.|382+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Dacite.|
27911|Theresa Creek Volcanics|71966|5|Briefly described|p989,1001|Late Devonian|Late Devonian|Geological province: Anakie Province, Thomson Orogen. Outcropping equivalent to felsic rhyolitic ignimbrite undercover in the Thomson Orogen; together with Mount Newsome Granodiorite, represents evidence for a middle Devonian c. 395-380 Ma felsic volcanic province.|382+\-7 Ma (MDA)|||||
27911|Theresa Creek Volcanics|73179|6|Mentioned|p1143|Late Devonian|Middle Devonian|Anakie Inlier.|||||Predominantly basaltic to andesitic.|
79724|Thomson beds|70673|5|Briefly described|p2, p10, p19-26, p41-47|||Carr et al. (2014). Maximum deposition age range c.496 - c.473 Ma.|494 +/- 15 Ma.||||Includes fine-grained, grey quartz sandstone.|
79724|Thomson beds|70744|5|Briefly described|p943|||Subsurface Thomson Orogen, southern and central Queensland. Contains abundant detrital zircons with Pacific-Gondwana signature.|495 Ma (maximum depositional age).||||Quartz-rich siliciclastic turbidites.|
79724|Thomson beds|70749|5|Briefly described|p43-52, p55|Cambrian|Ordovician|New, informal name. Undercover Thomson Orogen. Also appears as Thomson Beds in Fig.2 and p51-52. Moderate to deep marine turbidites. Very widespread grouping of deposits. Several almost identical age determinations given. Lu-Hf and O isotopic results discussed.  Maximum depositional age given from AAO Beryl 1 (beneath Galilee Basin) and DIO Naryilco 1, Tickalara 1:25k sheet area, Orientos 7241, SW Qld.|494 +/- 15 Ma, 496+/-16 Ma.||||Moderately to steeply dipping, interbedded argillite, siltstone to sandstone, graphitic shale and massive sandstone to greywacke.|23-APR-18
79724|Thomson beds|71031|6|Mentioned|p7|||Thomson Orogen.||||||
79724|Thomson beds|71251|6|Mentioned|p3|||Yowah-Cunnamulla area. Map symbol (Eth) implies Cambrian age inferred.||||||26-APR-18
79724|Thomson beds|71864|6|Mentioned|p3|||||||||
79724|Thomson beds|71965|4|Described|p896,899,905,906,911-913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Informal terminology of Carr et al. (2014) to include braod, widespread group of rocks throughout the undercover of Thomson Orogen in QLD. Of overall low magnetic intensity, mostly masked by overlying basins. Age constraints: 498+\-16 Ma (MDA); 425.4+\-6.6 Ma (Ella Belt intrusions). Best represented in stratigraphic drill holes GSQ Eromanga 1, GSQ Quilpie 1 and GSQ Thargomindah 1. Interpreted to be a turbiditic package, with foliation sub-parallel to bedding.|498 +/- 18 Ma (max dep age)|||Intruded by Ella Belt intrusions. Laterally grades into Lycosa Formation and Werewilka Formation. Correlable with Warratta Group, Tongo Formation, Twin Tanks Metamorphics, Nebine Metamorphics.|Monotonous interbedded metasandstone and metasiltstone.|29-OCT-19
79724|Thomson beds|71966|5|Briefly described|p989-990, p1000|Early Ordovician|Cambrian|Geological province: Thomson Orogen. Widespread package of dominantly low-grade, quartz-rich turbiditic metasedimentary rocks. Outcrops occur in Charters Towers and Anakie provinces, and undercover in the Thomson Orogen. Synchronous with widespread I- and S-type magmatism in the Thomson Orogen.||||Underlain by Machattie beds. Correlable with Warratta Group.||25-OCT-19
79724|Thomson beds|72522|4|Described|p1-2, p36, p62-63, 65, 70-77, 78, 86-93|Late Silurian|Cambrian|Thomson Orogen. U-Pb SHRIMP maximum depositional ages given for  sample 2169078 from GSQ Quilpie 1, 145.04083d E 26.6350d S and sample 2172123 from 143.469dE 28.2359dS (GDA94). A sandstone from GSQ Thargominda with max. dep. age of 497+/-10 Ma may also be part of the Thomson beds. Detrital zircon spectra compared with Glenroy Formation, but ~460 Ma component missing from Thomson beds. Minimum age constraints from Ella Granite, Wollgolla Granite. See also p81, p96, p101.|499+/-7 Ma, 508 +/- 15 Ma||||Monotonously interbedded metasandstone and metasiltstone interpreted as turbidites.|
79724|Thomson beds|73147|5|Briefly described|p143|||Thomson Orogen. Covered by Ealy to Middle Jurassic strata of the Eromanga and Surat Basins.|||||Metasedimentary rocks.|
79724|Thomson beds|73177|5|Briefly described|p1097, p1113 Fig.15, 1114, 1115 Fig.17|Early Ordovician|Cambrian|See also p1116. Southern Thomson Orogen. Deposited in a deep-marine setting outboard of the Delamerian continental margin (backarc basin deposits). Also appears as Thomson Beds in Fig.16.||||Possibly equivalent to Girilambone Group.||
24026|Thornborough Andesite Member|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Kungaree Volcanic Subgroup. Thickness: ~30m. Geological Province: Georgetown Region.||||||08-JUL-15
24026|Thornborough Andesite Member|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24026|Thornborough Andesite Member|40542|6|Mentioned|p97|||||||||
24026|Thornborough Andesite Member|43259|6|Mentioned|Appendix 1,p2.||Carboniferous|||||||
24026|Thornborough Andesite Member|43740|4|Described|p9|||||||||
24026|Thornborough Andesite Member|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Corkscrew Rhyolite (Kungaree Volcanic Subgroup).||||||
24026|Thornborough Andesite Member|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Also mapped separately are four variants, one of which is named as a Member.||Unit in Corkscrew Rhyolite.|||Greenish-grey to brown sparsely porphyritic pyroxene trachyandesite(?) to andesite; probably includes intrusive equivalents.|
70387|Thornhill Gabbro|65452|6|Mentioned|p6 Fig.2|Permian|Permian|||||||
70387|Thornhill Gabbro|67203|6|Mentioned|p6|Permian|Permian|||||||
70387|Thornhill Gabbro|68319|5|Briefly described|Map Legend|Permian|Permian||||||Dark grey to black, medium to coarse-grained gabbro; fine-grained equigranular diorite.|
70387|Thornhill Gabbro|68421|5|Briefly described|Map Legend|Late Permian|Late Permian||||||Dark grey to black, medium to coarse-grained gabbro; fine-grained equigranular diorite.|
70387|Thornhill Gabbro|68679|5|Briefly described|p421|||Gayndah-Gladstone belt.|||||Gabbro, diorite.|
70387|Thornhill Gabbro|73450|6|Mentioned|p22|||Interpreted to pre-date Borilla Granite.||||||
30015|Thornton Granite|23422|5|Briefly described|Plate 7.3|Late Permian|Late Permian|||||||
30015|Thornton Granite|23423|5|Briefly described|p311 Table 7.4||Late Permian|Pieter Botte Supersuite.||||||
30015|Thornton Granite|43070|2|Defined|p95|Late Permian||||||||
30015|Thornton Granite|43285|5|Briefly described|Map Legend||Late Permian|||||||
30015|Thornton Granite|43625|5|Briefly described|p52,128,Appendix 8|||||||||
30015|Thornton Granite|60425|5|Briefly described|p54 Tb. 4, p272-3 Appdx. 1|Late Permian|Early Permian|Of Nulbullul Suite (Pieter Botte Supersuite). Intruded Hodgkinson Formation and Obree Point Volcanics. I-type. Pale to medium grey, fine-grained, slightly porphyritic biotite leucogranite -- further lithological details included (p273).||||||07-FEB-11
30015|Thornton Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. ||Nulbullulul Suite.||||
36294|Three Horse Lagoon Granite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36294|Three Horse Lagoon Granite|69593|5|Briefly described|p484|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|320-280 Ma.||||Hornblende-biotite granodiorite to biotite granite and leucogranite. I-type.|
36240|Three Mile Microgranite|23423|5|Briefly described|p314 Table 7.4|Early Permian|Late Carboniferous|Claret Creek Supersuite.||||||
36240|Three Mile Microgranite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Claret Creek Ring Complex, Claret Creek Supersuite.||||||
36240|Three Mile Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 361. I-Type.||||||
36240|Three Mile Microgranite|23616|6|Mentioned|Table 3 p55|||See also p100 Appendix 2. Of Claret Creek Supersuite.||||||
36240|Three Mile Microgranite|60425|5|Briefly described|p51 Tb. 3, p282-3 Appdx. |Late Carboniferous|Late Carboniferous|Of Claret Creek Suite (Claret Creek Sup'ste). Also a part of Claret Creek Ring Complex. Cuts into Claret Creek Volcanics. Porphyritic biotite microgranite. I-type.||||||07-FEB-11
36240|Three Mile Microgranite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Porphyritic biotite microgranite.|
36240|Three Mile Microgranite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Claret Creek Supersuite.|||Porphyritic biotite microgranite.|
36393|Three Sisters Complex|23429|5|Briefly described|p447 Fig 13.26|Permian|Carboniferous|probably an area of mineralisation rather than a stratigraphic unit.||||||21-JAN-21
24032|Thunder Egg Rhyolite|23291|4|Described|p94 Tb. 3.9|Early Permian|Early Permian|Parent: Agate Creek Volcanic Group. Overlies, or downfaulted into, Etheridge Group. Thickness: ~ 900m. Geological Province: Georgetown Region.||||||08-JUL-15
24032|Thunder Egg Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V31. Assumed to be I-Type.||||||
24032|Thunder Egg Rhyolite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
24032|Thunder Egg Rhyolite|40542|6|Mentioned|p97|||||||||
24032|Thunder Egg Rhyolite|43259|4|Described|Appendix 1,p3.||Permian|of Agate Creek Volcanic Group.||||||
24032|Thunder Egg Rhyolite|43740|4|Described|p31||Carboniferous|||||||
24032|Thunder Egg Rhyolite|50199|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Agate Creek Volcanic Group.||||||
24032|Thunder Egg Rhyolite|50211|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Agate Creek Volcanic Group. Overlies Black Soil Andesite. Sparsely porphyritic rhyolite with locally abundant agate-filled spherulites.||||||14-MAY-04
24032|Thunder Egg Rhyolite|68353|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Conformably overlies Black Soil Andesite.|Brown to pink sparsely porphyritic rhyolite with locally-abundant agate-filled spherulites; probably includes intrusive equivalents.|
24032|Thunder Egg Rhyolite|68357|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.||Unit in Agate Creek Volcanic Group.||Conformably overlies Black Soil Andesite.|Brown to pink sparsely porphyritic rhyolite with locally-abundant agate-filled spherulites; probably includes intrusive equivalents.|
24032|Thunder Egg Rhyolite|72297|6|Mentioned|p755||||||||Spherulitic lavas containing thunder eggs.|
25529|Thunderbolt Granite|23162|5|Briefly described|p880||Permian|Excluded from new Urannah Suite as TG is compositionally distinct. Age: 277.9+/-6.3Ma.||||||
25529|Thunderbolt Granite|24521|5|Briefly described|p102|Permian|Permian|Age: 278+/-6Ma (zircon). Geological Province: New England Orogen.||||||
25529|Thunderbolt Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
25529|Thunderbolt Granite|31984|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25529|Thunderbolt Granite|32553|4|Described|p58|||||||||
25529|Thunderbolt Granite|32556|4|Described|Table 3|||L.Perm.||||||
25529|Thunderbolt Granite|35940|6|Mentioned|Fig.2|||||||||
25529|Thunderbolt Granite|36045|6|Mentioned|p333|||See also Fig.4.||||||
25529|Thunderbolt Granite|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
25529|Thunderbolt Granite|38365|6|Mentioned|p2|||||||||
25529|Thunderbolt Granite|39252|6|Mentioned|p21|||||||||
25529|Thunderbolt Granite|39445|5|Briefly described|Table 12|||||||||
25529|Thunderbolt Granite|41246|6|Mentioned|Map legend|Permian||||||||
25529|Thunderbolt Granite|44815|14|Not recorded|unknown (p313-346)|||265 Ma||||||
25529|Thunderbolt Granite|45087|5|Briefly described|p34|||Chemical analyses||||||
25529|Thunderbolt Granite|45151|5|Briefly described|Table 7|||||||||
25529|Thunderbolt Granite|48905|6|Mentioned|p28|||265m.y.||||||
25529|Thunderbolt Granite|48922|3|Fully described|p46|||||||||
25529|Thunderbolt Granite|60659|5|Briefly described|p19|||Possible an informal name? A mesozonal batholith of granite and granodiorite, with aplitic granite dykes.||||||07-FEB-11
25529|Thunderbolt Granite|60705|5|Briefly described|p647 Fig. 2, p661|Early Permian|Early Permian|Of the Thunderbolt Suite.||||||
25529|Thunderbolt Granite|65706|5|Briefly described|Tb.1 p15,16,18; p43, p65, p78|Early Permian|Early Permian|Contains amethyst mineralisation - crystals up to 20mm across and 30mm long have been found. Possible epithermal Au-Ag mineralisation.||||Intruded by Hecate Granite.|Hornblende-biotite granite, porphyritic microgranite, altered granodiorite, granitic gneiss, aplitic microgranite dykes.|
25529|Thunderbolt Granite|68679|5|Briefly described|p361, p363, p366-368|Permian|Permian|Northern Connors Subprovince. Early Permian. Post-tectonic intrusion. Forms prominent, massive unfoliated outcrops. Geochemical plots.|277.9 +/- 6.3 Ma (Allen et al., 1998).|Thunderbolt Suite.|||Fine- to medium-grained (sphene-)hornblende-biotite monzogranite, with scattered pale pink K-feldspar phenocrysts.|
25529|Thunderbolt Granite|69594|6|Mentioned|p570-571 Figs.7.44-45|||Northern Urannah Batholith. Geochemistry plots.||||||
25529|Thunderbolt Granite|70673|5|Briefly described|p5, p9, p118, p125, p127|Permian|Permian|Part of the Urannah Batholith. Forms prominent outcrops. Has well-developed foliation.|277.9 +/- 6.3 Ma (Allen et al., 1998).|||||
25529|Thunderbolt Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|278+/-6.3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
25529|Thunderbolt Granite|72297|6|Mentioned|p758|||At Binbee, between Bowen and Collinsville, amethyst and quartz crystals occur in weathered granite.||||||
25529|Thunderbolt Granite|73029|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, pale pinkish grey to pale pink, medium-grained, uneven-grained to moderately porphyritic hornblende-biotite monzogranite; with traces of titanite, clinopyroxene, allanite, and scattered mafic inclusions to 30cm (most <10cm).|
25529|Thunderbolt Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale grey, pale pinkish grey, or pale greyish pink to pale pink, med-grained, uneven-grained to moderately porphyritic hornblende-biotite monzogranite; w traces of titanite, clinopyroxene, allanite, + scattered mafic inclusions to 30cm (most <10cm).|
35541|Thunderbolt Suite|23162|5|Briefly described|p877|||Intrudes, along with Permian-Triassic mafic dykes, the Connors Arch which is composed of the Urannah Suite.||||||
35541|Thunderbolt Suite|23549|5|Briefly described|p525-528|Permian|Permian|Intrudes the Urannah Supersuite.  Age: 278Ma. (Allen et al 1998). In the Connors Arch (Queensland).  See also Fig. 17 p527.||||||05-APR-05
35541|Thunderbolt Suite|60705|6|Mentioned|p658|||Includes the Thunderbolt Granite.||||||
35541|Thunderbolt Suite|68679|5|Briefly described|p363|||Allen et al. (1998); one of their three Suites comprising the Carboniferous-early Permian Urannah Batholith. Geochemistry summarised.|||Thunderbolt Granite.||I-type.|
31113|Thursday Monzogranite|23032|5|Briefly described|p40|||||||||
31113|Thursday Monzogranite|23422|5|Briefly described|p215 Table 6.9|||||||||
31113|Thursday Monzogranite|43480|2|Defined|7-32|Devonian|Silurian|||||||
31113|Thursday Monzogranite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Pink, porphyritic muscovite-biotite monzogranite containing pink K-feldspar phenocrysts to 3 cm and locally intensely foliated to cataclastic.|
31113|Thursday Monzogranite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
39882|Ti Tree Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Geological Province: Mount Isa Block. Age: ~ 1518-1508Ma (U-Pb)||||||
39882|Ti Tree Granite|24257|5|Briefly described|p72 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological Province: Eastern fold belt, Mount Isa Block.||||||
39882|Ti Tree Granite|60665|6|Mentioned|p1157 Fig.9, |Calymmian|Calymmian|Northern Cloncurry intrusion. Age inferred from Fig.9.|1512 +/- 5 Ma.|||||
39882|Ti Tree Granite|66913|5|Briefly described|p171 fig 2|Calymmian|Calymmian|U-Pb zircon SHRIMP age shown diagramatically on Fig. 2.||||||
76898|Tick Hill Complex|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event||Wonga Suite, Burstall Suite|||Cream to pink, massive to strongly foliated, fine to medium-grained leucogranite; patches of coarser graphic to pegmatitic granite; local tourmaline and vuggy quartz zones; scattered calc-silicate granofels rafts and grey to pink granitic gneiss.|
76898|Tick Hill Complex|69591|5|Briefly described|p60|||Mount Isa Province.|||||Cream to pink, massive to strongly foliated, fine to medium leucogranite; irregular patches of coarse graphic to pegmatitic granite; local tourmaline and vuggy quartz zones; scattered calc-silicate granofels rafts and grey to pink granitic gneiss.|
76898|Tick Hill Complex|73413|6|Mentioned|p5, p8-9, p21-22|||[Also written as Tick Hill complex]. Includes rafts of the Corella Formation.||||Intrudes the Corella Formation.|Includes syn-tectonic granite sheets and gneisses.|
76898|Tick Hill Complex|73553|4|Described|p2, p20, p43-p45, p46-47,|Statherian|Orosirian|Mary Kathleen Domain. Very poorly exposed as several northerly trending lenses around Tick Hill mine. Included in Kalkadoon Granite on first edition 1:250 00-scale Duchess geological map (Carter and Opik, 1963), and subsequently Corella Formation by Blake et al., (1982a) except for one small lens. Delineated during GSQ-GA mapping of 2006-2009, briefly described by Hutton and Withnall (2013, Table 2.2, p60). Recent isotopic dating indicates granitoids were emplaced ~1850 Ma, and ~1770-1780 Ma in the case of deformed pegmatites. Pink to red tones on radiometric images, low aeromagnetic response. A-type. See also p49-54, p58, p253.|~1850 Ma and ~1770-1780 Ma (U-Pb zircon, LAICPMS)|||Intrudes Corella Formation|Pinkish grey to dark grey, fine- to medium-grained, moderately-highly porphyritic amphibole-biotite quartz monzonite. Highly deformed and metamorphosed, well-developed foliated.|03-FEB-23
22998|Ticklehim Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Wakara Volcanic Subgroup of Featherbed Volcanic Group.||||||
22998|Ticklehim Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V101. A-Type.||||||
22998|Ticklehim Rhyolite|23616|5|Briefly described|Table 5 p71||Permian|Age: 278+/-3 Ma (Rb-Sr). Of Featherbed Volcanic Group. Hodgkinson Province.||||||
22998|Ticklehim Rhyolite|23713|5|Briefly described|p23|||Age: 278+/-3 Ma (Rb-Sr). Of Featherbed Volcanic Group.||||||
22998|Ticklehim Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group||||||
22998|Ticklehim Rhyolite|43083|5|Briefly described|p92|||Rb-Sr age of 278+/-3 Ma.Of Featherbed Volcanic Group||||||
22998|Ticklehim Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group).  Crystal-rich rhyolitic ignimbrite. Age: 278+/-3Ma.||||||15-JUN-06
22998|Ticklehim Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Wakara Volcanic Subgroup. Age 278+/-3 Ma.||||||
22998|Ticklehim Rhyolite|43259|4|Described|Appendix 1,p10.||Permian|of Wakara Volcanic Subgroup. Age is 278+/-3 Ma.||||||
22998|Ticklehim Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
22998|Ticklehim Rhyolite|43625|6|Mentioned|p38|||Age: 278+/-3 Ma||||||
22998|Ticklehim Rhyolite|43626|2|Defined|p89||Early Permian|Rb-Sr Age: 278+/-3 Ma||||||
22998|Ticklehim Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
22998|Ticklehim Rhyolite|60425|5|Briefly described|p44 Tb. 3|Early Permian|Early Permian|Informal subunit of Wakara Volcanic Subgroup (Featherbed Volcanic Group) - known as the Ticklehim Creek Dyke Swarm (Morgan 1974; Oversby/AGSO, 1989; Mackenzie 1993). Age: 278+/-3Ma. (Rb-Sr).||||||07-FEB-11
22998|Ticklehim Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Included in Lags Supersuite.|278 Ma.|Featherbed Volcanic Group.|||A-type.|
27914|Tiger Hill Microgranite|23291|5|Briefly described|p99 Tb. 3.11|Late Carboniferous|Carboniferous|Of the Western Ingham Batholith (Cashmere area). Geological Province: Georgetown Region.||||||08-JUL-15
27914|Tiger Hill Microgranite|23494|5|Briefly described|p20 Tb. 1|Permian|Permian|Massive, pink medium-grained granite with some biotite.  Intrudes Herbert River Granite.||||||
27914|Tiger Hill Microgranite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 409. I-Type.||||||
27914|Tiger Hill Microgranite|23619|4|Described|p38 Table 2|Permian|Carboniferous|Herbert River Batholith.||||||
27914|Tiger Hill Microgranite|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
27914|Tiger Hill Microgranite|31832|6|Mentioned|Table 6|||||||||
27914|Tiger Hill Microgranite|32553|4|Described|p58|||||||||
27914|Tiger Hill Microgranite|39027|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
27914|Tiger Hill Microgranite|39445|5|Briefly described|Table 12|||||||||
27914|Tiger Hill Microgranite|43113|4|Described|Table 2 p24|Permian|Carboniferous|||||||
27914|Tiger Hill Microgranite|43253|5|Briefly described|map legend|Permian|Carboniferous|||||||
27914|Tiger Hill Microgranite|43259|4|Described|Appendix 1,p45.|Permian|Carboniferous|||||||
27914|Tiger Hill Microgranite|44048|14|Not recorded|Map Legend||Permian|(Triassic?)||||||
27914|Tiger Hill Microgranite|44059|14|Not recorded|p442(Tb)||Late Paleozoic|||||||07-NOV-08
27914|Tiger Hill Microgranite|44516|14|Not recorded|p33|||||||||
27914|Tiger Hill Microgranite|44542|2|Defined|p27|||Probably intrudes Herbert Granite.||||||
27914|Tiger Hill Microgranite|45009|14|Not recorded|p75,Tb.13,Pl.13|||Probably equivalent to Elizabeth Creek Granite.||||||
27914|Tiger Hill Microgranite|46845|6|Mentioned|Table 6|||||||||
75145|Timana diorite|60425|5|Briefly described|p62 Tb. 4|Late Ordovician|Ordovician|Informally named subunit of Mission Beach Granite Complex. I-type.||||||07-FEB-11
23003|Timber Top Volcanic Subgroup|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
23003|Timber Top Volcanic Subgroup|23423|4|Described|p306 Table 7.3|Early Permian|Late Carboniferous|Of the Featherbed Volcanic Group. Overlain by Mount Mulligan Coal Measures. Maximum thickness: 480 m.||||||22-APR-09
23003|Timber Top Volcanic Subgroup|24485|5|Briefly described|p43 Tb.7|Early Permian|Late Carboniferous|||||||
23003|Timber Top Volcanic Subgroup|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of the Featherbed Volcanic Group.||||||15-JUN-06
23003|Timber Top Volcanic Subgroup|43285|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Featherbed Volcanic Group.||||||
23003|Timber Top Volcanic Subgroup|43625|4|Described|p36|||||||||
23003|Timber Top Volcanic Subgroup|43626|4|Described|p42|Early Permian|Late Carboniferous|||||||
23003|Timber Top Volcanic Subgroup|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Geological Province: Kennedy Province.||||||
23003|Timber Top Volcanic Subgroup|60425|3|Fully described|p46 Tb. 3, p65-66|Early Permian|Late Carboniferous|Of Featherbed Volc.Gp.Contains Breccia Ck + Controversy Hill Rhyolites + 6 informal units.Unconform.on Hodgkinson Fm + Wallaroo rhyolite; overlain disconform'ly by Fisherman Rhyolite? + Mt Mulligan CM. Cut by Maneater Granodiorite. A-type. Detailed lith.||||||07-FEB-11
23003|Timber Top Volcanic Subgroup|62523|4|Described|p2, p3-4 (map/legend)|Early Permian|Late Carboniferous|Of Featherbed Volcanic Group. Previously of "Featherbed Volcanics". Includes:Controversy Hill and Breccia Ck Rhyolites as well as unnamed units. Unconformable on Hodgkinson Formation; overlain by Yongala Volcanic Subgroup.||||||07-FEB-11
24524|Tin Hill Quartzite Member|23291|4|Described|85 Tb. 3.6, p76|||Parent: Robertson River Subgroup. Thickness: up to 40m. Geological Province: Georgetown Region.||||||26-MAY-15
24524|Tin Hill Quartzite Member|35921|2|Defined|p36|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||26-MAY-15
24524|Tin Hill Quartzite Member|36937|6|Mentioned|p229|||||||||
24524|Tin Hill Quartzite Member|38714|5|Briefly described|p188|||||||||
24524|Tin Hill Quartzite Member|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24524|Tin Hill Quartzite Member|39924|6|Mentioned|Fig.3|||||||||
24524|Tin Hill Quartzite Member|41680|6|Mentioned|p113|||||||||
24524|Tin Hill Quartzite Member|41975|6|Mentioned|p436|||||||||
24524|Tin Hill Quartzite Member|43664|4|Described|p27|||||||||
24524|Tin Hill Quartzite Member|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Corbett Formation (Robertson River Subgroup).||||||07-NOV-08
24524|Tin Hill Quartzite Member|50537|6|Mentioned|p2.5, Table 2.1|||Of the Robertson River Subgroup (Etheridge Group). Geological Province: Georgetown Inlier.||||||19-AUG-04
24524|Tin Hill Quartzite Member|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Corbett Formation.|||White quartzite.|
24524|Tin Hill Quartzite Member|69591|5|Briefly described|p64-65|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. A single 5-40m thick folded layer forms a series of prominent ridges near the Robertson River.||Corbett Formation.|||Quartzite consisting almost entirely of quartz, with traces of muscovite and tourmaline; possibly metamorphosed chemical sediment (chert)?|
77801|Tinami Valley Granodiorite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
77801|Tinami Valley Granodiorite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink to greyish pink, fine-grained, moderately porphyritic hornblende-biotite granodiorite; granophyric; mafic inclusions (to ~ 45cm) locally abundant.|
77801|Tinami Valley Granodiorite|68679|5|Briefly described|p431-432|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region. Similar to felsic parts of Colosseum Quartz Monzodiorite.|||||Pink to greyish pink, fine-grained, equigranular to slightly porphyritic biotite and hornblende granodiorite to monzodiorite, with some tonalite and granite; locally abundant mafic inclusions.|
36714|Tinaroo Suite|23423|5|Briefly described|p311 Table 7.4||Early Permian|S-type granite. Of Tinaroo Supersuite.||||||
36714|Tinaroo Suite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Brodies Camp, Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36714|Tinaroo Suite|69593|5|Briefly described|p478-480, p505, p506 Fig.6.26, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~305 km2 at Lamb Range, SW of Cairns. Age poorly constrained. Geochemistry briefly described; similar to Whypalla Supersuite.|||Tinaroo Granite.||S-type. Slightly to moderately porphyritic, biotite granite, traces of late garnet.|
36714|Tinaroo Suite|72983|6|Mentioned|p1, p3, p22, p25|||Champion and Bultitude (2013a, b). Contains only the Tinaroo Granite.|||Tinaroo Granite|||
29982|Tinaroo Supersuite|23423|4|Described|p311 Table 7.4||Early Permian|Age: ~280 Ma (Rb-Sr). Also see p245.||||||
29982|Tinaroo Supersuite|23430|6|Mentioned|p493|||||||||
29982|Tinaroo Supersuite|23497|6|Mentioned|p34|||||||||
29982|Tinaroo Supersuite|23506|5|Briefly described|Map Legend||Early Permian|||||||
29982|Tinaroo Supersuite|23616|4|Described|p78-79||Permian|S-type granite. Hodgkinson Province.||||||
29982|Tinaroo Supersuite|43060|4|Described|p108|||||||||
29982|Tinaroo Supersuite|44246|6|Mentioned|Map Legend||Early Permian|||||||
29982|Tinaroo Supersuite|60425|3|Fully described|p56 Tb. 4, p80|Early Permian|Early Permian|Comprises just Tinaroo Granite. Age: ~280Ma (Rb-Sr). Intruded part of Hodgkinson Formation and Emerald Creek Microgranite. White to pale grey, medium-grained, slightly to moderately porphyritic, biotite granite; S-type. Age details on p80.||||||07-FEB-11
29982|Tinaroo Supersuite|62371|5|Briefly described|p472 Fig.3|Permian|Permian|S-type granite.||||||
29982|Tinaroo Supersuite|63140|6|Mentioned|p572 fig 3|Early Permian|Early Permian|||||||
29982|Tinaroo Supersuite|63154|5|Briefly described|p281 Fig. 3|Early Permian|Late Carboniferous|Geological province: Hodgkinson Province. S-type granites.||||||11-APR-07
29982|Tinaroo Supersuite|72983|6|Mentioned|p3, p25|||Bultitude and Champion (1992). Contains only the Tinaroo Granite [of the Tinaroo Suite?].|||Tinaroo Granite, [Tinaroo Suite]|||
73611|Tincat Road Metamorphics|68421|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province.||||Intruded by the Glen Eva Complex.|Biotite-rich gneiss, biotite-muscovite gneiss, muscovite leucogneiss; minor migmatite and pegmatite.|
26283|Tinchoo Formation|13497|3|Fully described|v, vi, viii, xii, p69 fig 6.1|Ladinian|Anisian|Cooper Basin. Originally defined by Powis (1989) who subdivided the unit into the Gilpeppee and Doonmulla Members in Queensland, however these members were not recognised in SA. Powis (1989) nominated one type section whilst Channon and Wood (1989) named another within the same well. Both authors also proposed seperate reference sections. Lithology in South Australia where it is thinned by erosion is also described. Maximum thickness of 109m in South Australuia. Petrography and lithology are discussed in some detail.  Interpreted to have been deposited in a low-sinuosity fluvial environment. Hosts oil in the James 1 well. Deposited by low-sinuosity river systems. Reservoir characteristics discussed. See also p104, p105, p110, p112-p114, p119, p157 tbl 10.1, p159, p161, p167, p170, p216.||Nappamerri Group|Includes the Gilpeppee and Doonmulla Members.|Conformably overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation, Poolowanna Formation or Hutton Sandstone.  Equivalent to the Walkandi Formation.|Interbedded brown-grey siltstone and light grey sandstone (Doonmulla Member) overlain by uniform dense light grey to green siltstone with minor coal seams and conglomerate beds.|
26283|Tinchoo Formation|13516|5|Briefly described|p164, p171 fig 12|Middle Triassic|Middle Triassic|In Cooper, Eromanga Basins.|||Includes Doonmulla Member, Gilpepee Member.|||
26283|Tinchoo Formation|22839|6|Mentioned|P33||Early Triassic|||||||
26283|Tinchoo Formation|22883|6|Mentioned|P29|Late Triassic|Middle Triassic|||||||
26283|Tinchoo Formation|22924|6|Mentioned|49|||||||||
26283|Tinchoo Formation|23155|6|Mentioned|p23|Mesozoic|Mesozoic|The Tinchoo Formation forms part of the Nappamerri Group, however it is not preserved on STRZELECKI.||||||
26283|Tinchoo Formation|23375|4|Described|Fig2 p265, 293|Ladinian|Anisian|In the Cooper Basin.||||||17-JAN-08
26283|Tinchoo Formation|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Middle Triassic|Of the Nappamerri Group.  Geological Province: Cooper Basin.||||||
26283|Tinchoo Formation|24282|6|Mentioned|p11|||Cooper-Eromanga Basin.||||||
26283|Tinchoo Formation|24372|5|Briefly described|p21|Triassic|Triassic|Geological Province: Cooper Basin.||||||
26283|Tinchoo Formation|42008|2|Defined|p271|Carnian|Anisian|Of Nappamerri Group.||||||
26283|Tinchoo Formation|42085|6|Mentioned|Fig.2 P374|||||||||
26283|Tinchoo Formation|43628|6|Mentioned|Fig.13|||||||||
26283|Tinchoo Formation|43711|6|Mentioned|p19||Triassic|||||||
26283|Tinchoo Formation|44133|4|Described|p65 Fig. 8.3, 86, 96|Upper Triassic|Triassic|Of the Nappamerri Group. Geological Province: Cooper Basin. Includes: Doonmulla Member, Gilpeppee Member. Conformably overlies Wimma Sandstone Member. Overlain by the Cuddapan Formation.||||||17-JAN-08
26283|Tinchoo Formation|60386|6|Mentioned|p299|Late Triassic|Early Triassic|Cooper/Eromanga Basin. Non-marine.||||||
26283|Tinchoo Formation|60717|5|Briefly described|p40 Fig. 2|Ladinian|Anisian|Of the Nappamerri Group. Overlies Arrabury Formation. Thickness: 100m. Geological province: Cooper Basin.||||||
26283|Tinchoo Formation|61015|6|Mentioned|p44|||||||||
26283|Tinchoo Formation|61613|5|Briefly described|p282 Fig. 2|Triassic|Early Triassic|Of Nappamerri Group. Includes Doonmulla and Gilpepee Members. Members. Underlain by Arrbury Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
26283|Tinchoo Formation|61614|6|Mentioned|p290 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||17-MAR-09
26283|Tinchoo Formation|61615|6|Mentioned|p302 Fig. 2|Late Triassic|Middle Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
26283|Tinchoo Formation|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||31-MAR-09
26283|Tinchoo Formation|62537|6|Mentioned|p191 Fig.2. |||Cooper Basin.||Unit in Nappamerri Group.||||
26283|Tinchoo Formation|62730|5|Briefly described|p352 Fig. 1|Late Triassic|Middle Triassic|Of the Nappamerri Group. Geological Province: Cooper Basin.||||||21-APR-08
26283|Tinchoo Formation|63978|2|Defined|p23, Fig. 3|Middle Triassic|Middle Triassic|Top of Nappamerri Gp. Unconformable on Arrabury Fm.; unconformable below Cuddapan Fm. Thickness: 263m. Interbedded sandstone, siltstone, mudstone, minor coal; sandstone is dominant in lower part, siltstone/mudstone/minor coal dominates upper section.||||||07-FEB-11
26283|Tinchoo Formation|64048|5|Briefly described|p64 Tb. 2|||Top unit of Nappamerri Group. Unconformable on Arrabury Formation. Geol.Prov: Cooper Basin. Comprises a fining-upwards succession with lower sublabile to quartzose fluvial sandstones (Doonmulla Member) and an upper sandstone-dominated Gilpeppee Member.||||||07-FEB-11
26283|Tinchoo Formation|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Middle Triassic|Cooper Basin. Underlies the Nappamerri Unconformity.||Unit in Nappamerri Group.||Overlies Wimma [Sandstone] Member (Arrabury Formation).||
26283|Tinchoo Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.|||Includes Doonmulla and Gilpeppee Members.|Overlies Arrabury Formation.||
26283|Tinchoo Formation|65238|5|Briefly described|p9|||Unconformably overlies the Arrabury Formation.||||||17-FEB-10
26283|Tinchoo Formation|65489|5|Briefly described|p15, p48-49, p55, p63, p96, p131, p150|Late Triassic|Middle Triassic|Cooper Basin. 100m thick. Oil reservoir accounting for 3% of the Basin's production.||Unit in Nappamerri Group.|Includes Gilpeppee and Doonmulla Members.|Overlies Arrabury Formation. May correlate with Peera Peera Formation.||
26283|Tinchoo Formation|67402|6|Mentioned|p90, p90 fig CPR4|||||Nappamerri Group|Includes the Doonmulla Member and Gilpeppee Member.|Unconformably overlies the Arrabury Formation.||
26283|Tinchoo Formation|68731|5|Briefly described|p200 Fig 3.110, p207, p208|Ladinian|Anisian|Powis (1989). Cooper Basin. ~ 125-200 m thick. Lower: highly sinuous fluvial environment. Upper: extensive fluvio-lacustrine environment. Palynofloras indicate Anisian-Ladinian (Gray and McKellar 2002).||Of the Nappamerri Group.|Includes the Doonmulla Member and the Gilpeppee Member.|Unconformably underlain by the Wimma Sandstone Member and the Arrabury Formation. Unconformably overlain by the Cuddapan Formation, and the Poolowanna Formation, or the Hutton Sandstone.|Comprises interbedded sandstone, silstone, mudstone and minor coal, with sandstone dominant in the lower part and siltstone, mudstone, and minor coal in its upper part.|
26283|Tinchoo Formation|69454|5|Briefly described|p38:4, 9|Ladinian|Anisian|Cooper Basin.||Nappamerri Group.||Uppermost part may be equivalent to Peera Peera Formation (Pedirka Basin).||12-JUL-16
26283|Tinchoo Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
26283|Tinchoo Formation|69673|6|Mentioned|p153 fig 125|||||Nappamerri Group||Overlies Arrabury Formation||
26283|Tinchoo Formation|69728|6|Mentioned|p285|||Cooper Basin.||Nappamerri Group.||||
26283|Tinchoo Formation|69797|5|Briefly described|p17 Fig.2, p18|Late Triassic|Middle Triassic|Oil reservoir. Age: Anisian - Carnian (approximated from figure). Geol. Prov: Cooper Basin. Presented in figure as Tinchoo Fm.||Nappamerri Group|||Oil reservoir.|
26283|Tinchoo Formation|69946|5|Briefly described|p9, p36, p54|Late Triassic|Middle Triassic|Cooper Basin.||Unit in Nappamerri Group.|Includes Doonmulla and Gilpeppee Members.|Conformably overlies Arrabury Formation. Is overlain unconformably by Cuddapan Formation.||
26283|Tinchoo Formation|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Middle Triassic|Cooper Basin.||Nappamerri Group.||||
26283|Tinchoo Formation|70317|6|Mentioned|p33|Middle Triassic|Middle Triassic|Cooper Basin.||Nappamerri Group.||Overlies Wimma Sandstone Member (Arrabury Formation). Is overlain unconformably by Cuddapan Formation.||
26283|Tinchoo Formation|70823|4|Described|iv, p40, p75-p79, p82|Middle Triassic|Middle Triassic|Cooper Basin. Deposited in sinuous meandering streams or fluviolacustrine environments. A maximum of 109m thickness is preserved in South Australia and a maximum 263m in Queensland. Outcrop and palynological characteristics are discussed.||Nappamerri Group|Includes the Gilpepee and Doonmulla members.|Conformably overlies the Wimma Sandstone Member (of the Arrabury Formation). Unconformably overlain by the Morney beds and Cuddapan Formation.|Planar cross-bedded, fine to medium grained sandstone with thin siltstone interbeds.|
26283|Tinchoo Formation|70824|5|Briefly described|p7, p9, p104|Ladinian|Anisian|Cooper Basin. Up to 109m thick. Deposited as sinuous meandering streams or fluviolacustrine environments.||Nappamerri Group|Includes the Doonmulla Member and the Gilpeppee Member.|Overlies the Wimma Sandstone Member (Arrabury Formation). Unconformably overlain by the Morney beds and Cuddapan Formation.||
26283|Tinchoo Formation|70946|5|Briefly described|p1089|Middle Triassic|Middle Triassic|Cooper Basin. Deposited in a sinuous meandering stream fluvio-lacustrine environment.||Nappamerri Group.||Overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation.||08-OCT-18
26283|Tinchoo Formation|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54|Carnian|Anisian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in Sinuous meandering streams or fluvio-lacustrine environments. See also  Ch7 p13, Ch13 p4, Ch13 p7-p8, Ch13 p36.||Nappamerri Group|Includes the Doonmulla Member and the Gilpeppee Member.|Overlies the Toolachee Formation. Overlies the Arrabury Formation. Unconformably overlain by the Cuddapan Formation.||
26283|Tinchoo Formation|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin.||Nappamerri Group||||
26283|Tinchoo Formation|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Callamurra Member, Panning Member and Wimma Sandstone Member , shown as floodplain, lacustrine, fluvial channels.||||||
26283|Tinchoo Formation|73251|6|Mentioned|p62|Middle Triassic|Middle Triassic|Cooper Basin. Sinuous meandering streams and fluviolacustrine depositional environments. Hydrocarbon source rock that contains[?] oil.||Nappamerri Group||Underlain by Arrabury Formation including Wimma Sandstone Member.||
26283|Tinchoo Formation|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin.||Nappamerri Group||Underlain by Wimma Sandstone Member.||
26283|Tinchoo Formation|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment. Major regional unconformity separates the overlying Eromagma Basin.|ca 238 Ma|Nappamerri Group||Overlies Wimma Sandstone Member, unconformably underlies Cuddapan Formation||
32132|Tindarra Granite|23037|4|Described|p76,7,8|Permian|Carboniferous|||||||
32132|Tindarra Granite|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgtd].  Pink to red, medium- to coarse-grained biotite granite.||||||09-SEP-14
32132|Tindarra Granite|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pink to red, medium- to coarse-grained, biotite granite.||||||18-MAY-04
32132|Tindarra Granite|65388|2|Defined|p277-278, p236 Fig. 81, p237, 238|Early Permian|Carboniferous|Appears to intrude the Torsdale Volcanics. May be intruded by the Glandore Granodiorite or may intrude it and the Shawlands Granodiorite Complex. Age uincertain. Pale red, medium to coarse grained, biotite syenogranite, potassically altered and fractured in north.||||||
32132|Tindarra Granite|68679|5|Briefly described|p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen.||||Intrudes Torsdale Volcanics. May intrude Shawlands Granodiorite Complex and Glandore Granodiorite; alternatively, may be intruded by Glandore Granodiorite.|Pink to red, medium-grained biotite granite.|
41374|Tinker Complex|60113|5|Briefly described|p14|Triassic|Triassic|Oil-bearing deposits in Silver Springs (Queensland).||||||
26174|Tinowon Formation|13516|6|Mentioned|p145 fig 3, p147 fig 5|Late Permian|Late Permian|From Roma Shelf, Bowen Basin. Age: APP5004 - APP5005||||||
26174|Tinowon Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26174|Tinowon Formation|23359|6|Mentioned|75|||||||||
26174|Tinowon Formation|24069|5|Briefly described|p284|Permian|Permian|Geological Province: Surat Basin.||||||
26174|Tinowon Formation|24077|5|Briefly described|p411 Tb. 3|Late Permian|Permian|Includes the Wallabella Coal Member.  Grey tuffaceous shale and siltstone, minor sandstone, thin tuff bands, rare coal seams, marine fossils common.  Max. thickness: 124m.  Geological Province: Bowen Basin.||||||
26174|Tinowon Formation|29391|6|Mentioned|Table 4|||Appears on P19.||||||
26174|Tinowon Formation|29721|6|Mentioned|Table 65|||||||||
26174|Tinowon Formation|32578|2|Defined|p353|Late Permian|Early Permian|Late Early to Late Permian||||||
26174|Tinowon Formation|36739|6|Mentioned|p22|||||||||
26174|Tinowon Formation|39445|5|Briefly described|Table 8|||||||||
26174|Tinowon Formation|39494|6|Mentioned|Fig.5|||||||||
26174|Tinowon Formation|40030|6|Mentioned|Fig.5|||||||||
26174|Tinowon Formation|40544|6|Mentioned|Fig.6|||||||||
26174|Tinowon Formation|41247|6|Mentioned|Fig.7|||||||||
26174|Tinowon Formation|41725|6|Mentioned|p403|||See also P410||||||
26174|Tinowon Formation|42250|6|Mentioned|Fig.3 p30|||||||||17-NOV-15
26174|Tinowon Formation|43000|5|Briefly described|p113|||||||||
26174|Tinowon Formation|45110|4|Described|Table 16|||See also Table 13.||||||
26174|Tinowon Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Includes the Wallabella Coal Member. Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
26174|Tinowon Formation|63713|5|Briefly described|p1507 Fig.2, p1528, p1531, p1535|Capitanian|Wordian|Roma Shelf, Bowen Basin. Shown as including Mantuan Productus Beds. Well-log correlation. A successful hydrocarbon exploration target.|||Includes Wallabella Coal Member.|Overlies Muggleton Formation. Is overlain by Black Alley Shale. Correlated with Peawaddy Formation.|Includes glacial diamictites.|
26174|Tinowon Formation|64665|6|Mentioned|p52.|Permian|Permian|Bowen Basin.||||||
26174|Tinowon Formation|64856|4|Described|p42, p56, p64-66|Late Permian|Late Permian|Paten and Groves (1974). Bowen Basin. Conformably overlies Muggleton Formation. Overlain by Black Alley Shale. Correlated with basal Burunga Formation. Contains Wallabella Coal Member. Age from palynoflora (unit APP5). Up to 88m thick. Shale, siltstone, some sandstone, coal.| | ||||29-NOV-17
26174|Tinowon Formation|64857|5|Briefly described|p119-121, p113 Fig.3|Late Permian|Late Permian|Western Bowen Basin. Contains the Wallabella Coal Member. Overlies Muggleton Formation.||||||
26174|Tinowon Formation|64858|5|Briefly described|p181 Tb. 1, p180 Fig.2, p182|Late Permian|Late Permian|Bowen Basin. Includes Wallabella Coal Member.||||||30-NOV-09
26174|Tinowon Formation|64859|6|Mentioned|p196, 225|Permian|Permian|Oil and gas source rocks.||||||
26174|Tinowon Formation|65115|5|Briefly described|p415, 416, 418|Tatarian|Tatarian|Deltaic unit on Roma Shelf. Equivalent to Scotia Coal Member, Taroom Trough.||||||
26174|Tinowon Formation|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
26174|Tinowon Formation|67402|4|Described|p18 fig WSD2, p19 fig WSD3, WSD4|Capitanian|Capitanian|Bowen Basin. Misspelt as the Tinowan Formation on p21 fig STC2 and p45 fig BWG3 and p56 tbl BWS2. Proven hydrocarbon reservoir and potential carbon dioxide storage reservoir. Deposited in a fluvial to fluvial-deltaic environments. See also p21, p30, p42 tbl HPB1, p45, p48, p53, p55, p56, p61, p62, p144, p301.||||Overlain by the Black Alley Shale. Unconformably overlies the Arbroath beds.|Shale, siltstone, quartzose sandstone, coal and tuff.|
26174|Tinowon Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Black Alley Shale/Winnathoola CM. Underlain by Muggleton Formation.||
26174|Tinowon Formation|68679|5|Briefly described|p377, p381-384|Permian|Permian|Paten and Groves (1974). Roma Shelf, Bowen Basin. 99m thick. Delta deposits. Has a shelly bed at its top, similar to the Black Alley Shale. Properties of the coal are described in some detail. Produces condensate-rich gas.||||Overlies Muggleton Formation. Is overlain by Black Alley Shale.|Shale, siltstone, fine- to medium-grained, poorly sorted quartzose sandstone, coal and tuff; marine fossils throughout.|
26174|Tinowon Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of  Bowen Basin. CA-TIMS age of 256.01 and 256.5 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||Unit of Wallabella Coal Member.|Includes Norambah Coal Measures.|||
26174|Tinowon Formation|70878|4|Described|p718, p720, p725|Permian|Permian|Bowen Basin. Calibration of palynological ages.|256.01 +/- 0.07 Ma.||Wallabella Coal Member.|Overlies Muggleton Formation. Is overlain by Black Alley Shale.|Includes tuff layers.|
26174|Tinowon Formation|70940|5|Briefly described|p844 Fig.1.|Permian|Permian|The only reference to this unit is in Fig.1 where it is presented as Lower Tinowon Formation and Upper Tinowon Formation.|c.259-256 Ma.|Blackwater Group.||Is overlain by Black Alley Shale.||
26174|Tinowon Formation|71863|6|Mentioned|p2|Paleozoic|Paleozoic|||||||
26174|Tinowon Formation|72297|6|Mentioned|p744-745|||Western Bowen Basin. Sandstones in this unit are hydrocarbon reservoirs.||||||
26174|Tinowon Formation|73304|5|Briefly described|p65, p67, p71-72, p78|||Dating by U-Pb CA-TIMS from upper part of unit.|256.01+/-0.30 Ma, 256.50+/-0.30 Ma||Wallabella Coal Member|||
26174|Tinowon Formation|73305|6|Mentioned|p548, p552|Late Permian|Late Permian|Roma Shelf. Regionally passes into the Fair Hill Formation. Time equivalent to the Fair Hill Formation and Peawaddy Formation.|||Mantuan Productus Beds in upper part, Wallabella Coal Measures in lower part|Equivalent to the Peawaddy Formation, Fair Hill Formation||
26174|Tinowon Formation|73625|6|Mentioned|p3, p5 Fig.3, p18|Permian|Permian|Roma Shelf, Western Bowen Basin.||||||
36531|Tintarple granite|23291|4|Described|p34,p89 Tb. 3.7|Proterozoic|Proterozoic|Informal name - see Candlow Formation. Has been equated with Forsayth granite (Smart & Bain, 1977). Geological Province: Georgetown Region.||||||08-JUL-15
36531|Tintarple granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 826.  S-Type.||||||
69005|Tireen Granite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Slightly foliated, grey to pink, fine to coarse-grained, mostly equigranular biotite monzogranite; some pink biotite leucogranite and minor coarse-grained hornblende gabbro.||||||
69005|Tireen Granite|65388|2|Defined|p335, p301 Fig 98, p318|Early Triassic|Late Permian|New unit. Previously mapped as part of the Delubra Gabbro. Outcrop poor and mostly very weathered. Cuts Tandora Granodiorite outcrop in two. Age inferred. Most commonly grey to pink, fine to coarse-grained, equigranular, biotite monzogranite with sparse black mafic enclaves to 5cm. Geophysical response does not match current mapped boundaries. These may need revision. Parts are similar to Greystone Granodiorite and Tandora Granodiorite.||||||
69005|Tireen Granite|68679|5|Briefly described|p419|||Rawbelle Batholith. ~20 km2.|||||Biotite monzogranite to syenogranite; comprises multiple rock types: may be composite. Slight foliation locally.|
29976|Tirrabella Supersuite|23503|5|Briefly described|Map Legend||Early Silurian|||||||
29976|Tirrabella Supersuite|23616|5|Briefly described|Table 1C p16, p67||Early Silurian|Age: 430 Ma. Hodgkinson Province.||||||
29976|Tirrabella Supersuite|43060|4|Described|p91|||||||||
29976|Tirrabella Supersuite|44246|5|Briefly described|Map Legend||Early Silurian|||||||
36267|Tirrabella Tonalite|23503|5|Briefly described|Map Legend||Early Silurian|of Tirrabella Supersuite.||||||
24035|Titania Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of O'Briens Creek Supersuite.||||||01-JUN-09
24035|Titania Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
24035|Titania Granite|41235|6|Mentioned|Fig.2a|||||||||
24035|Titania Granite|41740|6|Mentioned|p222|||||||||
24035|Titania Granite|43259|6|Mentioned|Appendix 1,p34.||Carboniferous|Of Emuford/Emu Granite.||||||01-JUN-09
24035|Titania Granite|60425|4|Described|p288-9 Appdx.|Late Carboniferous|Late Carboniferous|Unassigned to suite/supersuite. Pale pink, fine-grained to pegmatitic, porphyritic, granophyric (topaz-) biotite granite. Included in Emuford Granite on most recent maps. I-type.||||||07-FEB-11
26948|Tiverton Formation|22593|6|Mentioned|Table 1|||||||||
26948|Tiverton Formation|22973|5|Briefly described|p9 Fig.2 (b)|Early Permian|Early Permian|||||||
26948|Tiverton Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
26948|Tiverton Formation|23037|6|Mentioned|p59|||||||||
26948|Tiverton Formation|23042|5|Briefly described|p55||Permian|||||||
26948|Tiverton Formation|23052|5|Briefly described|Map Legend|Permian|Permian|||||||
26948|Tiverton Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
26948|Tiverton Formation|23161|4|Described|p28 table4|Early Permian|Early Permian|||||||
26948|Tiverton Formation|23430|5|Briefly described|p515|||||||||
26948|Tiverton Formation|29436|6|Mentioned|p317|||||||||
26948|Tiverton Formation|29437|6|Mentioned|p136|||Permian||||||
26948|Tiverton Formation|29441|6|Mentioned|p113|||||||||
26948|Tiverton Formation|31598|6|Mentioned|p31|||||||||
26948|Tiverton Formation|31690|6|Mentioned|p36|||||||||
26948|Tiverton Formation|32943|6|Mentioned|p106|||||||||
26948|Tiverton Formation|32945|6|Mentioned|p78|||See also PP79,80,89 & Fig.2. Permian||||||
26948|Tiverton Formation|32946|6|Mentioned|p910|||Bivalves||||||
26948|Tiverton Formation|32949|6|Mentioned|p441|||||||||
26948|Tiverton Formation|32950|6|Mentioned|Table 31.1|||||||||
26948|Tiverton Formation|33711|6|Mentioned|p383|||Table 3.||||||
26948|Tiverton Formation|34132|6|Mentioned|p2|||Lower Permian||||||
26948|Tiverton Formation|35284|6|Mentioned|Fig.1|||||||||
26948|Tiverton Formation|35467|6|Mentioned|p177|||||||||
26948|Tiverton Formation|35530|6|Mentioned|p1|||Location of Bivalvia fossils.||||||
26948|Tiverton Formation|36739|6|Mentioned|Fig.2|||||||||
26948|Tiverton Formation|37400|6|Mentioned|Table 2|||||||||
26948|Tiverton Formation|37458|6|Mentioned|p440|||||||||
26948|Tiverton Formation|37612|6|Mentioned|p282|||||||||
26948|Tiverton Formation|38505|6|Mentioned|p1115|||||||||
26948|Tiverton Formation|38586|6|Mentioned|p40|||||||||
26948|Tiverton Formation|38917|6|Mentioned|p156|||||||||
26948|Tiverton Formation|39220|6|Mentioned|p42|||Fauna II||||||
26948|Tiverton Formation|39261|6|Mentioned|Fig.6|||||||||
26948|Tiverton Formation|39262|4|Described|p121|||||||||
26948|Tiverton Formation|39267|4|Described|p232|||||||||
26948|Tiverton Formation|39273|6|Mentioned|p305|||||||||
26948|Tiverton Formation|39304|6|Mentioned|Photo 19.1|||||||||
26948|Tiverton Formation|40093|6|Mentioned|p35|||||||||
26948|Tiverton Formation|40571|5|Briefly described|p31|||||||||
26948|Tiverton Formation|40997|6|Mentioned|p413|||||||||
26948|Tiverton Formation|41034|5|Briefly described|p367|||||||||
26948|Tiverton Formation|41191|6|Mentioned|Fig.3|||||||||
26948|Tiverton Formation|41246|6|Mentioned|Map legend|Permian||||||||
26948|Tiverton Formation|41315|6|Mentioned|p148|||||||||
26948|Tiverton Formation|41666|6|Mentioned|p20|||||||||
26948|Tiverton Formation|41689|6|Mentioned|Table 1|||||||||
26948|Tiverton Formation|42249|6|Mentioned|Table 1 P22|||||||||
26948|Tiverton Formation|42250|6|Mentioned|Fig.4 P31|||||||||
26948|Tiverton Formation|42257|5|Briefly described|Table 1 P263|||||||||
26948|Tiverton Formation|42258|4|Described|p275|||||||||
26948|Tiverton Formation|42422|6|Mentioned|p325|||Bowen Basin||||||
26948|Tiverton Formation|42654|6|Mentioned|p14|||||||||
26948|Tiverton Formation|42701|3|Fully described|p62|||||||||
26948|Tiverton Formation|42865|6|Mentioned|p18|||||||||
26948|Tiverton Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
26948|Tiverton Formation|42994|6|Mentioned|p43|||||||||
26948|Tiverton Formation|43000|6|Mentioned|p107|||||||||
26948|Tiverton Formation|43018|5|Briefly described|Table 1,p386|||||||||
26948|Tiverton Formation|43050|5|Briefly described|p4|||||||||
26948|Tiverton Formation|43213|6|Mentioned|p152|||Represents a major marine transgression.||||Conformably overlies Reids Dome beds.||
26948|Tiverton Formation|43475|14|Not recorded|p552,553||Permian|||||||
26948|Tiverton Formation|43882|14|Not recorded|p87-89,91,93,97|||(Nebo) Ammonoids.||||||
26948|Tiverton Formation|43894|14|Not recorded|p788|||||||||
26948|Tiverton Formation|44000|2|Defined|Tb.1,2,p22,29-33,58,||Early Permian|Overlies Lower Bowen Volcanics; Underlies Gebbie Formation. Basal unit of Middle Bowen Beds. p64||||||
26948|Tiverton Formation|44245|5|Briefly described|Map Legend||Permian|||||||
26948|Tiverton Formation|44409|14|Not recorded|Map Legend||Permian|||||||
26948|Tiverton Formation|44424|14|Not recorded|p293-301|||Now Tiverton Subgroup.||||||
26948|Tiverton Formation|44489|14|Not recorded|p69|||=Unit A.||||||
26948|Tiverton Formation|44513|14|Not recorded|p59-63||Permian|||||||
26948|Tiverton Formation|44635|4|Described|p10,11,Tb.1,map||Early Permian|||||||
26948|Tiverton Formation|45031|14|Not recorded|p6|||Of Back Creek Group||||||
26948|Tiverton Formation|48881|2|Defined|p1,8,12,20-24,Tb.1||Early Permian|||||||
26948|Tiverton Formation|60115|5|Briefly described|p21 Fig. 1|Early Permian|Early Permian|Geological Province: northern Bowen Basin.||||||04-FEB-08
26948|Tiverton Formation|60472|5|Briefly described|Map Legend|Late Permian - Correct|Early Permian|Of the Back Creek Group.  Lithic sandstone, coquinite, calcareous sandstone and siltstone, conglomerate.||||||29-SEP-04
26948|Tiverton Formation|60659|5|Briefly described|p20||Early Permian|Of Back Creek Gp. Micaceous very fine- to medium-grained, thin- to medium-bedded lithic sst, siltst, mudst, coquinite + minor conglomerate. Disconformably or unconformably overlies Lizzie Creek Volcanic Gp. Geol Prov: Bowen Basin.||||||07-FEB-11
26948|Tiverton Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||17-MAR-09
26948|Tiverton Formation|61917|5|Briefly described|Map legend|Late Permian|Early Permian|Of the Back Creek Group. Lithic sandstone, coquinite, calcareous sandstone and siltstone, conglomerate; fossiliferous.||||||
26948|Tiverton Formation|65388|4|Described|p185-187, 126, 149, 159, 166,173,178,179|Artinskian|Asselian|Of Back Creek Group in northern Bowen Basin. Originally defined by Malone & others (1966). Raised to Subgroup status in 1973, but the Subgroup fell into disuse and Formation reinstated, based on original type section, ~225m thick. From 225-630m thick. Time equivalent to Collaroy Volcanics and Buffel Formation based on fossils. Represents major marine transgression. Overlies Lizzie Creek Volcanic Group. Overlain by Gebbie Formation. Artinskian age is more consistent with the SHRIMP date of the underlying Mount Benmore Volcanics (284.7+/- 4.4Ma)||||||
26948|Tiverton Formation|65706|6|Mentioned|p15 Tb.1, p16 Tb.1|Late Permian|Early Permian|Possibly unconformably overlies Lizzie Creek Volcanic Group. ||Of Back Creek Group.||||
26948|Tiverton Formation|67402|4|Described|p21, p45, p80|Kungurian|Artinskian|Bowen Basin. See also p80 tbl BWN1, p84, p85 tbl BWN2, p165 tbl LPB1.||Back Creek Group||Overlies the Lizzie Creek Volcanics. Overlain by the Gebbie Formation and the Collinsville Coal Measures.|Lithic sandstone, coquinite, calcareous sandstone and siltstone, and conglomerate.|
26948|Tiverton Formation|67669|5|Briefly described|p11|Early Permian|Early Permian|Of Bowen Basin.||||Overlain by Collinsville Coal Measures. Underlain by Lizzie Creek/Bulgonunna volcanics.||
26948|Tiverton Formation|68679|5|Briefly described|p353, p358, p360, p378-381|Artinskian|Artinskian|Malone et al. (1966). Connors-Auburn Province. Bowen Basin. 700m thick. Transgressive shallow-marine shelf deposits. RELATED UNITS (continued): Time-equivalent of and interfingers with Collaroy Volcanics. Passes laterally into Collinsville Coal Measures.||Back Creek Group.||Overlies Mount Benmore Volcanics. Is transitional with the upper Lizzie Creek Volcanic Group. Is overlain by Gebbie Formation. Correlated (probably) with Yatton Limestone. See COMMENTS for more.|Lithic sandstone, coquinite, calcareous sandstone and siltstone.|
26948|Tiverton Formation|73036|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Lithic sandstone, coquinite, calcareous sandstone and siltstone, conglomerate; fossiliferous.|
26948|Tiverton Formation|73037|5|Briefly described|Map legend|Late Permian|Early Permian|||Back Creek Group|||Lithic sandstone, coquinite, calcareous sandstone and siltstone, conglomerate; fossiliferous.|
38863|Tollbar Breccia|24488|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex. Coarse breccia, clasts dominantly altered granitoid.||||||
38863|Tollbar Breccia|24489|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Glassford Igneous Complex.||||||
38863|Tollbar Breccia|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kggt].  Coarse breccia, clasts dominantly altered granitoid.||||||
38863|Tollbar Breccia|68008|3|Fully described|p442, p444, p453-456, p460, p635|Early Cretaceous|Early Cretaceous|Noted and mapped (as Breccia phase) by Neale (1968). Occurs W of Mount Sugarloaf, between Ridler Creek and Tollbar Creek, after which it is named and which constitutes the type area. Forms low hills. Geophysics briefly described and modelled. Presumably is derived by brecciation of the Ridler Monzonite.||Glassford Igneous Complex.||Is entirely surrounded by (?intrudes) Ridler Monzonite.|Coarse breccia with angular to rounded clasts (mainly but not exclusively) of altered granitic rocks in a limonitic matrix. A number of different type of breccia are present (well illustrated).|
38863|Tollbar Breccia|68553|6|Mentioned|Map legend|Cretaceous|Cretaceous|This unit, as well as the Burns Spur Nepheline Monzosyenite, Judas Trachybasalt, Radley Nepheline Syenite, Ridler Monzonite, Goondicum Gabbro, and unnamed intrusive units, are all mapped under the symbol, Kgs.||||||
38863|Tollbar Breccia|73450|6|Mentioned|p11|||||||||
70389|Tolson Creek Igneous Complex|65452|6|Mentioned|p6 Fig.2, p22, p29|Late Triassic|Late Triassic|Part of Agnes Water Caldera Complex. High-level emplacement. Geochemistry briefly described.||||||
70389|Tolson Creek Igneous Complex|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Subdivided lithologically into two unnamed units|||||Dark grey to black medium-grained diorite and gabbro; fine-grained white and black net-veined hornblende granodiorite with gabbro inclusions; pink medium to coarse-grained equigranular syenogranite, granodiorite and monzogranite.|
70389|Tolson Creek Igneous Complex|68679|5|Briefly described|p428, p433|Late Triassic|Late Triassic|Northern New England Orogen; Agnes Waters area.|||||Dark grey to black, medium-grained diorite and gabbro; fine-grained, white, net-veined hornblende granodiorite with gabbro enclaves; pink, medium- to coarse-grained, equigranular syenogranite, granodiorite and monzogranite.|
26176|Tommy Creek Microgranite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|1625+/-4Ma [probably U/Pb SHRIMP age].||||||16-MAR-18
26176|Tommy Creek Microgranite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1760Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
26176|Tommy Creek Microgranite|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26176|Tommy Creek Microgranite|30531|6|Mentioned|p18|||Also mention P20 and P22.||||||
26176|Tommy Creek Microgranite|32660|5|Briefly described|Table 5|||||||||
26176|Tommy Creek Microgranite|33900|5|Briefly described|p23|||||||||
26176|Tommy Creek Microgranite|35167|2|Defined|p154|Middle Precambrian|Middle Precambrian|||||||
26176|Tommy Creek Microgranite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
26176|Tommy Creek Microgranite|36052|6|Mentioned|p433|||||||||
26176|Tommy Creek Microgranite|37568|6|Mentioned|p85|||||||||
26176|Tommy Creek Microgranite|38235|6|Mentioned|p115|||||||||
26176|Tommy Creek Microgranite|38833|6|Mentioned|p161|||||||||
26176|Tommy Creek Microgranite|39202|6|Mentioned|p230|||||||||
26176|Tommy Creek Microgranite|39445|6|Mentioned|p43|||1607 Ma. See also Table 2||||||
26176|Tommy Creek Microgranite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
26176|Tommy Creek Microgranite|45166|5|Briefly described|p43|||||||||
26176|Tommy Creek Microgranite|49041|5|Briefly described|Table 3|||Mention Table 4||||||
26176|Tommy Creek Microgranite|50100|5|Briefly described|p13 Fig.4|Statherian|Statherian|Intrudes the Tommy Creek beds.||||||
26176|Tommy Creek Microgranite|50332|5|Briefly described|p16, p21, p68|Proterozoic|Proterozoic|Intrudes the "Tommy Creek beds". Consists of a series of felsic sills, and comprise rhyolitic metavolcanics and leucogranite.||||||22-JUL-13
26176|Tommy Creek Microgranite|50536|5|Briefly described|p1.5, 11.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Tommy Creek Suite.||||||
26176|Tommy Creek Microgranite|61926|5|Briefly described|p73 Fig. 3|||Possibly an informal reference to a microgranite within the Tommy Creek beds? ||||||
26176|Tommy Creek Microgranite|64248|6|Mentioned|p38 Fig.5|Statherian|Statherian||1625 +/- 4 Ma.|||Intrudes Tommy Creek Beds.||11-DEC-17
26176|Tommy Creek Microgranite|64250|6|Mentioned|p11 fig 3, p21|Statherian|Statherian|Cloncurry Fold Belt, Mount Isa Inlier.|1625 +/-4 Ma|||||13-MAY-14
26176|Tommy Creek Microgranite|65396|6|Mentioned|p82, p175, p191, p241|Statherian|Statherian|Tommy Creek Block, Mount Isa Inlier.|1625 +/- 4 Ma|||Intrudes Tommy Creek Beds.||
26176|Tommy Creek Microgranite|67323|5|Briefly described|GIS attrib tbl, p16-17, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. Derrick (1980). Tommy Creek Domain, Mount Isa Inlier. Tommy Creek Igneous Event. Included felsic volcanics that are now assigned to Bulonga Volcanics. High Th radiometric response.|1650 +/- 3 Ma (OZCHRON database).|||Intrudes Corella Formation. Is overlain unconformably by Milo beds.|Pink, saccharoidal, equigranular to porphyritic leucocratic microgranite with minor biotite; commonly weakly foliated.|
26176|Tommy Creek Microgranite|67539|6|Mentioned|p12|||||||Probably unconformably overlain by Milo beds, rather than intruding them.||
26176|Tommy Creek Microgranite|68542|6|Mentioned|p1 |||||||||
26176|Tommy Creek Microgranite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
26176|Tommy Creek Microgranite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
26176|Tommy Creek Microgranite|69056|5|Briefly described|p2, p4, p6, p14 Tb.3, p18, p23, p28, p56|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Tommy Creek Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area. Modelling values listed.|1653 +/- 4 Ma (Geoscience Australia, 2010).|||Intrudes the Corella Formation. Correlated with the Mount Isa Group.|Weakly foliated, equigranular to porphyritic, leucocratic microgranite.|
26176|Tommy Creek Microgranite|69591|5|Briefly described|p28, p43, p45, p47, p59|Paleoproterozoic|Paleoproterozoic|Tommy Creek Domain, Isa Superbasin. Is coeval with the Mount Isa Group. A 1660 +/- 6 Ma MDA of the overlying unit suggests it is part source for the Milo beds.|1653 +/- 4 Ma and 1650 +/- 3 Ma (OZCHRON).|||Intrudes Corella Formation. Is overlain nonconformably by Milo beds.|Pink, saccharoidal, equigranular to porphyritic leucocratic microgranite with minor biotite; commonly weakly foliated.|
26176|Tommy Creek Microgranite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink, saccharoidal, equigranular to porphyritic leucocratic microgranite with minor biotite; commonly weakly foliated.|
26176|Tommy Creek Microgranite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink, saccharoidal, equigranular to porphyritic leucocratic microgranite with minor biotite; commonly weakly foliated.|
26176|Tommy Creek Microgranite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1625+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
26176|Tommy Creek Microgranite|72889|6|Mentioned|p6 Fig.i.|||||||||
26176|Tommy Creek Microgranite|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
26176|Tommy Creek Microgranite|73413|6|Mentioned|p3|Statherian|Statherian|Mount Isa Inlier, Eastern Fold Belt.|1625 +/- 4 Ma|||||
26176|Tommy Creek Microgranite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mitakoodi-Tommy Creek Domain.|1654+/-4 Ma crystallisation age||||Felsic intrusive.|
31440|Tommy Creek Suite|50536|5|Briefly described|p1.2, 1.5, 11.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1760Ma.||||||07-NOV-08
75665|Tommy Roundback Granodiorite|68679|5|Briefly described|p362|Mississippian|Mississippian|Northern Connnors Subprovince. Unfoliated.|323.1 +/- 2.2 Ma (SHRIMP U-Pb: Cross et al., 2012)|||||
75665|Tommy Roundback Granodiorite|68901|5|Briefly described|p4, p22-24, p25, p27, p144|Late Carboniferous|Early Carboniferous|northern New England Orogen Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.
|323.1 +/- 2.2 Ma (SHRIMP U-Pb)|||Intrudes the Milwarra Quartz Diorite.|White, fine- to medium-grained, slightly porphyritic biotite-hornblende granodiorite.|15-NOV-18
75665|Tommy Roundback Granodiorite|70673|5|Briefly described|p5, p123|Late Carboniferous|Late Carboniferous|Indistinguishable from ages for adjacent Milwarra Quartz Diorite and Ward Creek Granodiorite.|323.1 +/- 2.2 Ma (Cross et al., 2012).|||||
75665|Tommy Roundback Granodiorite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|323+/-2.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
75665|Tommy Roundback Granodiorite|73197|5|Briefly described|p468|Carboniferous|Carboniferous|New England Orogen, northern. Similar to S-type granites, description from Cross et al., (2015) but has not been catagorised into A, S or I type. Shown as Tommy Roundback Granite p468 Fig.4.|323 Ma zircon age||||Muscovite-biotite monzogranite containing ovoid mafic inclusions.|
36491|Toms Creek rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 80.||||||
31114|Toms Hole Granodiorite|23032|5|Briefly described|p40|||||||||
31114|Toms Hole Granodiorite|23422|5|Briefly described|p215 Table 6.9|||Of Toms Hole Supersuite.||||||
31114|Toms Hole Granodiorite|43480|2|Defined|7-34|Devonian|Silurian|||||||
31114|Toms Hole Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey, medium-grained porphyritic epidote-sphene-hornblende-biotite granodiorite, with quartz phenocrysts to 1 cm and sparse equant plagioclase phenocrysts to 1.5 cm.|
31114|Toms Hole Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey, medium-grained porphyritic epidote-sphene-hornblende-biotite granodiorite, with quartz phenocrysts to 1 cm and sparse equant plagioclase phenocrysts to 1.5 cm.|
31114|Toms Hole Granodiorite|69592|5|Briefly described|p281, p283, p285|||Reedy Springs Batholith, Charters Towers Province. Geochemistry described in some detail.||Toms Hole Supersuite.|||Foliated, porphyritic hornblende-biotite granodiorite; with accessory titanite, epidote, zircon, apatite. I-type.|
38183|Toms Hole Supersuite|23422|4|Described|p178, p215 Table 6.9|||Possibly Devonian.  Intrudes the Cape River Metamorphics.||||||
38183|Toms Hole Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester and Upland Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
38183|Toms Hole Supersuite|69592|5|Briefly described|p280-281, p283, p285|||Reedy Springs Batholith, Charters Towers Province. Geochemistry described; contrasted with the White Springs Supersuite.|||Toms Hole Granodiorite.||Foliated, porphyritic hornblende-biotite granodiorite. I-type.|
35207|Toobier Granite|23042|6|Mentioned|Fig 2|||Misspelling of Mount Toobier Granite?||||||10-SEP-19
35207|Toobier Granite|60473|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Augite-hornblende-biotite quartz monzonite to monzogranite; augite-hornblende-biotite quartz monzodiorite.||||||
35207|Toobier Granite|60475|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Pinkish grey, medium grained, augite-hornblende-biotite quartz monzonite to monzogranite; monzodiorite.||||||
35207|Toobier Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35207|Toobier Granite|61035|4|Described|p9 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Mount Whelan + Mountain View Volcanics. Geological Province: Connors Sudprovince. Conists of medium-grained, augite-hornblende-biotite quartz monzonite to monzogranite.||||||07-FEB-11
35207|Toobier Granite|65388|2|Defined|p359-360, p90 Fig. 37, p94, 98|Late Carboniferous|Late Carboniferous|Connors Province.  Interpreted to intrude Mountain View Volcanics, Whelan Creek Volcanics. Age uncertain. Pinkish-grey, medium-grained, biotite quartz monzonite to monzogranite.||||||
35207|Toobier Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus, Tooloombah Creek and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
35207|Toobier Granite|68679|5|Briefly described|p347, p356|Carboniferous|Carboniferous|Northern New England Orogen.||||Intrudes Whelan Creek Volcanics.||
25542|Toolburra Silt|42593|5|Briefly described|p301|||||||||
75135|Toolgbar granite|60425|4|Described|p98, p100, p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name for felsic granite of Bedarra Suite (Bedarra Batholith or Supersuite? in Bedarra Granite Belt.Occurs on Wheeler Island. Pale grey, medium-grained, moderately porphyritic biotite granite; with scattered biotite-rich clots (to~3cm). I-type.||||||07-FEB-11
35131|Tooloombah Creek Granite|23042|4|Described|p68,9||Carboniferous|Intrudes Connors Volcanics. Overlying unit Leura Volcanics (un).||||||28-MAY-08
35131|Tooloombah Creek Granite|60480|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Light greenish grey to pink, medium grained, equigranular biotite granite, locally granophyric.||||||
35131|Tooloombah Creek Granite|61035|4|Described|p10 Tb. 1|Late Carboniferous|Late Carboniferous|Intrudes Broadsound and Clive Creek Volcanics and unconformably overlain by Leura Volcanics. Geological Province: Connors Sudprovince. Light greenish grey to pink, medium-grained, equigranular biotite granite, locally granophyric.||||||07-FEB-11
35131|Tooloombah Creek Granite|65388|2|Defined|p360-361, p86 Fig. 35, p102 Fig. 42|Late Carboniferous|Late Carboniferous|Connors Province. Intrudes Clive Creek Volcanics and Broadsound Range Rhyolite. Overlain by Leura Volcanics. Relationships indicate age. Mainly of light greenish grey to pink, medium-grained, equigranular biotite granite.||||||
35131|Tooloombah Creek Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus,Toobier and Waitara Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
35131|Tooloombah Creek Granite|68679|5|Briefly described|p347, p357 Fig.5.42|Carboniferous|Carboniferous|Northern New England Orogen. See also reference to Tooloombah Granite (p356).||||Intrudes Broadsound Range Volcanics. Is overlain nonconformably by Leura Volcanics.||
29067|Toomba Basalt|23032|6|Mentioned|p48|Quaternary|Quaternary|Could be as young as 13000 BP.||||||
29067|Toomba Basalt|23352|4|Described|291|||||||||
29067|Toomba Basalt|23498|5|Briefly described|p19  table 1|Recent|Late Pleistocene|Olivine basalt. Uncomformably overlies Nulla Basalt.||||||
29067|Toomba Basalt|23505|5|Briefly described|Map legend||Quaternary|||||||
29067|Toomba Basalt|23508|5|Briefly described|Map Legend||Quaternary|||||||
29067|Toomba Basalt|30151|4|Described|p22|||Pleistocene age. Table 3 on P22.||||||
29067|Toomba Basalt|31285|5|Briefly described|p88|||Age||||||
29067|Toomba Basalt|31832|6|Mentioned|Table 6|||||||||
29067|Toomba Basalt|32553|4|Described|p34|||||||||
29067|Toomba Basalt|33644|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
29067|Toomba Basalt|33648|6|Mentioned|p23|||Strat.||||||
29067|Toomba Basalt|33958|4|Described|p42|||Late Tert. - Quat.  See also PP43-49.||||||
29067|Toomba Basalt|34046|6|Mentioned|Table III|||||||||
29067|Toomba Basalt|34409|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
29067|Toomba Basalt|36472|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
29067|Toomba Basalt|36561|6|Mentioned|Fig.1|||||||||
29067|Toomba Basalt|39027|6|Mentioned|Map legend|Recent|Recent|||||||
29067|Toomba Basalt|39686|6|Mentioned|p69|||||||||
29067|Toomba Basalt|39731|6|Mentioned|p31|||||||||
29067|Toomba Basalt|39735|6|Mentioned|p20|||||||||
29067|Toomba Basalt|40623|5|Briefly described|p91|||||||||
29067|Toomba Basalt|41244|6|Mentioned|p31|||||||||
29067|Toomba Basalt|41537|6|Mentioned|Fig.2|||||||||
29067|Toomba Basalt|43286|5|Briefly described|Map Legend||Quaternary|||||||
29067|Toomba Basalt|44049|14|Not recorded|Map Legend||Recent|||||||
29067|Toomba Basalt|44060|14|Not recorded|Map Legend||Quaternary|||||||
29067|Toomba Basalt|44061|4|Described|Table 6||Quaternary|||||||
29067|Toomba Basalt|44800|14|Not recorded|p16,22,map|Recent|Pleistocene|late Pleistocene-early Recent.||||||
29067|Toomba Basalt|45009|14|Not recorded|p91,92,101||Recent|Similar to Kinrara Basalt.||||||
29067|Toomba Basalt|45151|5|Briefly described|p23|||See also Table 12.||||||
29067|Toomba Basalt|48903|3|Fully described|p35|||Table 4. Recent ?||||||
29067|Toomba Basalt|48904|4|Described|p70|||||||||
29067|Toomba Basalt|48914|4|Described|p52|||Late Tert. - Quat.  ?Recent.||||||
29067|Toomba Basalt|69599|5|Briefly described|p633|||West of Charters Towers.|~10 ka (Stephenson et al., 1978).|||||
29067|Toomba Basalt|73115|5|Briefly described|p:16, 25, 75-78, 83-84, 86, 112,123,129|Pleistocene|Pleistocene|[Also written as Toomba Basalt Flow]. Nulla Basalt Province, southern. Lava flow is 120 km long. Includes [rare?] evidence for pyroclastic behaviour. Highly vesicular; includes large vesicles up to 6 cm wide, and basal vesicular zones. Has no soil development and retains a primary jagged blocky surface and ropey pahoehoe textures. Elevated above the surrounding sedimentary landscape by 7 m. Typically associated with rainforests and vine thickets [helpful for remote identification]. Unit has significance for groundwater processes. [Also written as Toomba Basalt Flow in all diagrams]|13-20 ka|||||
39154|Toonboro Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Strongly altered and silicified, medium-grained, equigranular hornblende granodiorite.|
39154|Toonboro Granite|68679|5|Briefly described|p433|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Strongly altered and silicified, medium-grained, equigranular hornblende granodiorite.|
39154|Toonboro Granite|73450|6|Mentioned|p16|||||||||
23025|Top Pinnacle Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group and Burton Lagoon Granite||||||
23025|Top Pinnacle Granite|43596|4|Described|p31, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Oswald Schist and Artella Granite(?). Variable textures and contacts described.||||||15-JAN-09
23025|Top Pinnacle Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
36314|Torpys Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
36314|Torpys Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale grey to pinkish grey, fine- to medium-grained, hornblende-biotite monzogranite.|
36369|Torres Strait Volcanic Group|23421|4|Described|Tb 5.3 p164|||Intruded by Badu Suite. Also see p160.||||||
36369|Torres Strait Volcanic Group|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Elimeek and Wallaman Falls Volcanics; Janet Ranges, Koolmoon and Silent Creek Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
36369|Torres Strait Volcanic Group|69593|5|Briefly described|p476-477|||Willmott et al. 91969).||Badu Suite.|||Dominantly rhyolitic, allanite- and biotite-bearing volcanic rocks. Hornblende and rare pyroxene have been reported in the rhyolites, as well as some andesites.|
36369|Torres Strait Volcanic Group|71031|5|Briefly described|p2-p3, p38, p41, p43|Early Permian|Early Carboniferous|Oriomo Province. Previously correlated with the Janet Ranges Volcanic Group. Outcrops in the Bluff Quarry area, 9km west-southwest from the tip of Cape York.|353.4 +/- 2.2 Ma ||Includes the Eborac Ignimbrite and Endeavour Strait Ignimbrite.|Intrudes the Endeavour Strait Ignimbrite (or the Eborac Ignimbrite).|Feldspar-quartz porphyry.|
36369|Torres Strait Volcanic Group|72983|5|Briefly described|p4-5, p61-62, p64|Carboniferous[?]|early Carboniferous|Jardine Subprovince, Kennedy Igneous Association. Previously considered broadly co-magmatic with the Badu and Horn Island granites. New age data indicates the unit represents an older, distinct magmatic event that broadly correlates with the oldest documented magmatism of the Kennedy Igneous Association.||Badu Supersuite|Endeavour Strait Ignimbrite, Eborac Ignimbrite, Goods Island Ignimbrite, Muralug Ignimbrite|||
35006|Torsdale Volcanics|23037|4|Described|p17,30-40,66,71,|Late Carboniferous|Early Carboniferous|Replaces Torsdale beds("").  Intruded by granites of the Rawbelle Batholith. Overlying unit Camboon Volcanics (un).||||||
35006|Torsdale Volcanics|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Cvt].  Dacitic to rhyolitic ignimbrite and other volcaniclastic rocks and lava; subordinate andesitic rocks; volcanilithic conglomerate and sandstone.||||||
35006|Torsdale Volcanics|50214|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
35006|Torsdale Volcanics|50215|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Overlain by Camboon Volcanics. Dacitic to rhyolitic ignimbrite and other volcaniclastic rocks and lava.||||||18-JUN-09
35006|Torsdale Volcanics|50273|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
35006|Torsdale Volcanics|50301|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
35006|Torsdale Volcanics|50597|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Dacitic to rhyolitic ignimbrite, minor porphyritic rhyodacitic to rhyolitic lava, rare andesite.||||||
35006|Torsdale Volcanics|50598|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Dacitic to rhyolitic ignimbrite, porphyritic rhyodacitic to rhyolitic lava, rare andesite.||||||
35006|Torsdale Volcanics|60282|5|Briefly described|p4||Nammalian|Formerly the Torsdale beds. Of the Connors-Auburn Volcanic Arch.  Ages: 313+/-6, 316+/-6 and 324+/-4 Ma (Withnall et al 1998).||||||
35006|Torsdale Volcanics|61777|5|Briefly described|p223, p227, p228, p225 Tab. 1|Early Carboniferous|Late Devonian|Replaces Torsdale beds. Overlain by Mount Bulgi Conglomerate Member). Age: 313+/-6 and 316+/-6Ma (SHRIMP U/Pb). Geological Province: Yarrol Province.Mostly rhyolite to dacite. See p227 for detailed info.||||||07-FEB-11
35006|Torsdale Volcanics|65388|3|Fully described|p13-20, 11, 14, 20, p27, 28, 29|Late Carboniferous|Early Carboniferous|Auburn Arch.  Ages: 325+/- 4 Ma to 298+/-5.1 Ma, U/Pb SHRIMP. Earlier included in the Permian "Camboon Andesite"; "Torsdale beds" of Dear and others (1971). Disconformably overlain by Camboon Volcanics. Contacts may be diachronous. Unconformably overlain by Precipice Sandstone, Evergreen Formation. Intruded by Glandore Granodiorite. Predominantly rhyolitic to dacitic ignimbrite, lava, and related epiclastic sediments. Sometimes difficult to distinguish from Camboon Volcanics. Forms inlier to Jurassic Evergreen Formation at Mount Misery. Correlated with Youlambie Conglomerate. See also p166, 236, p244, 248, 250, 252, 284, 301, 340, 432, 447.||||||
35006|Torsdale Volcanics|68008|5|Briefly described|p132||||298.2 +/- 5.1 Ma (SHRIMP: Withnall et al., 2009).|||Is overlain by Mount Bulgi Conglomerate or Camboon Volcanics.|Includes rhyolitic ignimbrite and comagmatic granites.|
35006|Torsdale Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Auburn Subprovince.||||||
35006|Torsdale Volcanics|68679|5|Briefly described|p312-313, p351-355, p407-408, p419, p469|Pennsylvanian|Pennsylvanian|Dear et al. (1971). Southern part of the Connors-Auburn Volcanic Arc, northern New England Orogen. Forms a N-trending belt. Mostly undeformed and dips shallowly. Probably fluvial and lacustrine deposits in a volcanic landscape. Possibly comagmatic with Nine Mile Granite. RELATED UNITS (continued): Is intruded by Berri Berri, Broadlands, Dogherty, Dawson, Glenleigh, Hutchinsons, Jan Mar, Kandoonan, Nine Mile, Rockdale, Ross, Tindarra and (inferred) Glenhalvern Granites; Delusion, Rockybar Granodiorites; Okangal Quartz Monzodiorite; Wind Mill Diorite; Parraweena, Kooyong Gabbros; Woolton Granite Complex; and probably by Ah Fat Granodiorite Complex.|~325-300 Ma.|||Flanked and overlain by the Camboon Volcanics. See COMMENTS for list of intruding units.|Mainly crystal-rich rhyolitic to dacitic ignimbrite with subordinate spherulitic lava, and related epiclastic sediments; locally massive ignimbrite; andesitic or basaltic rocks relatively uncommon, locally as volcanic sandstone and conglomerate.|
35006|Torsdale Volcanics|70033|6|Mentioned|p2, p29|||Unit at base of Bowen Basin.||||||
35006|Torsdale Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Porphyry, rhyolite, ignimbrite.|
35006|Torsdale Volcanics|73197|5|Briefly described|p465 Fig.4, p467|Carboniferous|Carboniferous|New England Orogen, northern. Auburn Subprovince. Unit belongs to the Currabubula-Connors Arc. Equivalent to the Connors Volcanic Group in the Connors Subprovince.|||||Predominantly rhyolitic to dacitic ignimbrites with minor lava flows, rare andesitic and basaltic lavas and volcaniclastic rocks.|
77843|Toweran Granodiorite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||White, fine-grained, leucocratic, moderately porphyritic biotite-hornblende and (hornblende-) biotite granodiorite; commonly partly altered.|
77843|Toweran Granodiorite|68679|5|Briefly described|p433|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||White, fine-grained, leucocratic, moderately porphyritic biotite-hornblende to biotite granodiorite; commonly partly altered; distinctly primitive and unevolved with many chemical characteristics of adakites.|
73897|Towgon Grange Suite|71628|5|Briefly described|p9-36|||||Clarence River Supersuite.|Towgon Grange Tonalite.|||
24534|Townley Formation|22533|6|Mentioned|p55|||In Georgetown Region||||||
24534|Townley Formation|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the Mt Isa Toole Creek Volcanics and Willyama Supergroup Bijerkerno Metasediments.||||||07-NOV-08
24534|Townley Formation|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon). Thickness: 400-1500m. Geological Province: Georgetown Region.||||||08-JUL-15
24534|Townley Formation|35921|2|Defined|p37|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24534|Townley Formation|36153|6|Mentioned|Fig.10|||||||||
24534|Townley Formation|36216|6|Mentioned|p208|||||||||
24534|Townley Formation|36780|6|Mentioned|Fig.10|||||||||
24534|Townley Formation|36937|6|Mentioned|p229|||||||||
24534|Townley Formation|38714|6|Mentioned|p182|||See also P18, 189. Comformably overlies Lane Creek Formation.||||||10-JUN-04
24534|Townley Formation|39445|5|Briefly described|Table 2|||||||||
24534|Townley Formation|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24534|Townley Formation|39924|6|Mentioned|Fig.3|||||||||
24534|Townley Formation|41975|6|Mentioned|p432|||||||||
24534|Townley Formation|42199|5|Briefly described|Table 1 P280|||||||||
24534|Townley Formation|43664|4|Described|p29|||||||||
24534|Townley Formation|50199|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Robertson River Subgroup (Etheridge Group).||||||07-NOV-08
24534|Townley Formation|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Etheridge Group.  Overlies: Lane Creek Formation.  Underlies: Heliman Formation.||||||07-NOV-08
24534|Townley Formation|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||19-AUG-04
24534|Townley Formation|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Etheridge Group. Overlies: Lane Creek Formation.  Underlies: Heliman Formation.||||||07-NOV-08
24534|Townley Formation|63866|6|Mentioned|p75|||Forsayth Subprovince, Etheridge Province.||Etheridge Group||||
24534|Townley Formation|65887|6|Mentioned|p45 Tb.2|||Includes schist. Sm-Nd isotopic data and depleted mantle model age.||||||
24534|Townley Formation|66800|6|Mentioned|p926 Table 1.|||||||Is overlain by Heliman Formation.||
24534|Townley Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||Upper Etheridge Group.||||
24534|Townley Formation|67341|5|Briefly described|vi, p14-17|||Forsayth Subprovince, Etheridge Province. Maximum depositional age.|1650 +/- 6 Ma (SHRIMP U-Pb zircon).|||Is overlain by Heliman Formation.|Fine-grained siltstone and sandstone.|
24534|Townley Formation|67430|6|Mentioned|p25|||||||||
24534|Townley Formation|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Etheridge Group.||Conformably overlies Lane Creek Formation. Is overlain conformably by Heliman Formation.|White to grey sericitic or lithic-quartz siltstone and fine sandstone, locally carbonaceous; minor quartzose siltstone and sandstone; carbonaceous siltstone (middle); white laminated sericitic siltstone and sandstone (base).|19-MAY-15
24534|Townley Formation|68353|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||Unit in Robertson River Subgroup.||Conformably overlies Lane Creek Formation.|Mica schist and quartzite derived from siltstone and fine lithic sandstone, locally carbonaceous.|
24534|Townley Formation|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Includes a separately mapped facies variant. Shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Etheridge Group.||Conformably overlain by the Heliman Formation. Conformably overlies Lane Creek Formation.|White to grey seritic or lithic-quartz siltstone and fine sandstone, locally carbonaceous; minor quartzose siltstone and sandstone; carbonaceous siltstone (middle); white laminated seritic siltstone and sandstone (base); mica schist and quartzite.|
24534|Townley Formation|69582|5|Briefly described|p76|||Etheridge Province. 40-150m thick. Intersected in GSQ Georgetown 8-9R.||||Overlies the Robertson River Subgroup. Overlain by the Heliman Formation.|Light grey siltstone, mudstone and sandstone.|
24534|Townley Formation|69591|4|Described|p61-62, p65, p67-68|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. 400-1500m thick. In the eastern limits of outcrop it grades into fine-grained mica schist. Contains significant population of ~1655-1650 Ma zircons (Neumann and Kositcin, 2011). Detrital zircon spectra.|~1650 Ma.|Etheridge Group.||Overlies Lane Creek Formation (Robertson River Subgroup).|White to pale grey siltstone, mudstone, and fine-grained quartzose to feldspathic sandstone (containing mudclasts). A conspicuous interval in mid-Formation of thin-bedded, well-laminated carbonaceous, locally calcareous siltstone to mudstone.|
24534|Townley Formation|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1650+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24534|Townley Formation|71799|6|Mentioned|p156||||ca <1650 Ma|||Overlies the Cobbold Metadolerite.||
34358|Townshend Formation|22740|5|Briefly described|155,163,164|Paleozoic|Paleozoic|Geol Province New England Fold Belt.||||||07-NOV-08
34358|Townshend Formation|61035|5|Briefly described|p14|||Geological Province: Wandilla Province. Multiply deformed and of high metamorphic grade, epidote-amphibolite, and included amphibolite, metaqyartzite and schist.||||||07-FEB-11
34358|Townshend Formation|65388|5|Briefly described|p153|||Of Curtis Island Group. Metabasalt, chert and quartz-rich turbidites. Broome Head Metamorphics are considered high grade equivalents.||||||
34358|Townshend Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Coastal Subprovince. This unit, as well as Broome Head, Duckpond Road and Gaythorn Metamorphics, Sabina Point Schist, The Shacks Mylonite, and metamorphic equivalents of Curtis Island Group, are all mapped under the symbol, DCcm.||||||
34358|Townshend Formation|68679|5|Briefly described|p309, p312-313, p319, p347|Carboniferous|Late Devonian|Morand (1993), Leitch et al. (1994). Townshend Island, Stanage Bay.||Curtis Island Group.||Equivalent to Broome Head Metamorphics.|Multiply-deformed, epidote-amphibolite grade metaquartzite, schist and amphibolite.|
34358|Townshend Formation|69952|6|Mentioned|p75|Carboniferous|Devonian|||||||
79125|Tozer Basalt Member|70913|4|Described|p8 fig 3, p9, p11, p41-p44, App 1 maps|Middle Permian|Early Permian|Gympie Province. Replaces the informal Tozer volcanics. Named for Tozer Street near the Gympie railway station. Often abreviated to Tozer Basalt (p37, 40, 41, 42, 43, 49, 53).Type locality and representative underground samples are briefly mentioned. A reference drill hole is also mentioned and distribution is briefly discussed. Up to 100m thick. See also p53, p67 fig 9.||At base of Mary Basalt.||Overlies the Kidgell Andesite Member. Intrudes the Dawn Formation.Tozer intrusions have probably fed both Tozer and Mary lavas. Occurs throughout stratigraphic package below Mary basalts.|Green pyroxene-phyric basalt flows, dykes and sills with no hematite. Basalts may be amygdaloidal and flanked by proximal hyaloclastites.|19-SEP-17
38208|Trafalgar Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Ordovician|||||||
38208|Trafalgar Supersuite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
34983|Tralee seam|23034|6|Mentioned|24|||Parent Rangal Coal Measures||||||
24041|Tregony Conglomerate Member|39969|6|Mentioned|p9|||||||||
24041|Tregony Conglomerate Member|40542|6|Mentioned|p98|||||||||
82692|Treverton Leucogranite|71628|5|Briefly described|p5: 1, 9-11|Permian|Permian|New name; after nearby Treverton Creek. A small (0.5 km2) intrusion ~56 km W of Stanthorpe, 2.5 km ENE of Warroo Station. Poorly exposed and deeply weathered; forms scattered boulders and boulder rubble. Possibly early Permian. Limited geochemistry described.||Mount You You Suite.||Intrudes Texas beds.|Dark pinkish-grey to pink, fine- to medium-grained, moderately porphyritic leucogranite; minor endoskarn. I-type.|
36396|Trevethan Granodiorite|23423|5|Briefly described|p251 +252||Permian|Age: 259+/-1 Ma. Yates Supersuite||||||
36396|Trevethan Granodiorite|23511|5|Briefly described|Map Legend||Late Permian|of Yates Supersuite. Age: 259 +/- 1Ma.||||||
36396|Trevethan Granodiorite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Yates Supersuite.  Age: 259 +/- 1Ma (Rb-Sr).||||||
36396|Trevethan Granodiorite|60425|5|Briefly described|p91, p272-3 Appdx. 1|Late Permian|Late Permian|See also Trevethan Granite. Of Trevethan Suite (Yates Supersuite). I-type. Age: 259+/-1Ma (Rb-Sr wh.rock biotite). Mainly med-gr., slightly to locally highly highly porph.orthopyroxene-clinopyroxene-hornblende-biotite granodiorite - lithol.detail on p273||||||07-FEB-11
36396|Trevethan Granodiorite|69593|5|Briefly described|p480, p482 Fig.6.6, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out at Black Mountain, S of Cooktown. Sm-Nd isotope data tabulated.|259 +/- 1 Ma.|Yates Supersuite.|||I-type.|
69330|Trevethan Suite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Yates Supersuite. Contains Trevethan Granodiorite and the informal Black Mountain granite. I-types.||||||07-FEB-11
27592|Tribute Hills Arenite|23032|4|Described|p18,19||Ordovician|||||||
27592|Tribute Hills Arenite|23424|4|Described|Table 8.1 Fig 8.2 p331||Ordovician|Age: unfossiliferous but probably Ordovician because of similarities to Judea Fm. Probably faulted against Greenvale, Pelican Range and Perry Creek Formations. Overlying unit Clarke River Group (u). Camel Ck Subprovince.||||||
27592|Tribute Hills Arenite|23430|5|Briefly described|p476|||Age uncertain, inferred to be Ordovician. Broken River Province.||||||
27592|Tribute Hills Arenite|23509|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Broken River Province.||||||
27592|Tribute Hills Arenite|23893|5|Briefly described|p14|Ordovician|Ordovician|Geological Province: Camel Creek Subprovince.||||||
27592|Tribute Hills Arenite|42690|5|Briefly described|map legend|Early Devonian|Ordovician|Variation on Tribute Hills Sandstone.||||||
27592|Tribute Hills Arenite|42692|5|Briefly described|map legend|Ordovician||||||||
27592|Tribute Hills Arenite|42752|5|Briefly described|p45|||see also Fig.2 p46||||||16-NOV-22
27592|Tribute Hills Arenite|42933|3|Fully described|p23|||||||||
27592|Tribute Hills Arenite|43095|5|Briefly described|Plate 2|||||||||
27592|Tribute Hills Arenite|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
27592|Tribute Hills Arenite|67848|6|Mentioned|p3 Fig.2.|||Part of the accretionary wedge in the arc-trench gap succession involved in collisional accretion.||||||
27592|Tribute Hills Arenite|68339|5|Briefly described|Map legend.|||Camel Creek Subprovince. Age max: Late Ordovician? Age min: Early Silurian?|||||Quartzose arenite, subordinate mudstone.|08-JUL-15
27592|Tribute Hills Arenite|68340|5|Briefly described|Map legend.|||Camel Creek Subprovince. Age max: Late Ordovician? Age min: Early Silurian?|||||Quartzose arenite, subordinate mudstone.|08-JUL-15
27592|Tribute Hills Arenite|68350|5|Briefly described|Map legend.|||Camel Creek Subprovince, Broken River Province. Age max: Late Ordovician? Age min: Early Devonian?|||||Quartzose arenite, subordinate mudstone.|08-JUL-15
27592|Tribute Hills Arenite|68351|5|Briefly described|Map legend.|||Camel Creek Subprovince, Broken River Province. Age max: Late Ordovician? Age min: Early Devonian?|||||Quartzose arenite, subordinate mudstone.|08-JUL-15
27592|Tribute Hills Arenite|68553|6|Mentioned|Map legend; schematic diagram.|Silurian|Ordovician|Broken River Province. This unit, as well as Pelican Range, Wairuna and Carriers Well Formations and Everetts Creek Volcanics, are all mapped under the symbol, OSb.||||||
27592|Tribute Hills Arenite|68576|5|Briefly described|Q_11: p38, p40|||Camel Creek Subprovince. Forms hilly topography. Source of clasts for an unnamed conglomerate in the basal Clarke River Group.|||||Quartzose sediments.|
27592|Tribute Hills Arenite|69030|6|Mentioned|p6|Ordovician|Ordovician|Camel Creek Subprovince (Broken River Province).||||||
27592|Tribute Hills Arenite|69079|6|Mentioned|p5|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.||||||
27592|Tribute Hills Arenite|69592|5|Briefly described|p251 Fig.4.35, p270, p277, p297|Devonian|Late Silurian|Camel Creek Subprovince, Broken River Province. A fault-bounded belt. Forms a dissected upland. Similar age and context to Pelican Range Formation: both are sandwiched between the Greenvale and Perry Creek Formations. Unfossiliferous.|||||Thick- to very thick-bedded, commonly amalgamated, fine-grained to very fine-grained, quartzose sandstone. Melange zones common.|
27592|Tribute Hills Arenite|73201|4|Described|p607, p610-611, p614, p616, p618, p620|Early Ordovician|Cambrian|Mossman Orogen, Broken River Province. Geochron is a U-Pb LA-ICP-MS detrital zircon maximum depositional age. Dominant detrital zircon peaks represent the Pacific-Gondwana and Grenville clusters common throughout Ordovician and older units of the Tasmanides. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Age given as late Cambrian to Early Ordovician.|484.4 +/- 6.2 Ma||||Quartzose greywacke with uncommon melange and pre-slaty cleavage folding. Dominated by intervals of thick to very thick bedded, fine to very coarse sandstone.|
36343|Trig Hill Granite|22460|6|Mentioned|p455|||Prospect O42, Cloncurry goldfield.||||||
24044|Trooper Creek Formation|22621|6|Mentioned|p203,218|Ordovician|Cambrian|part of Seventy Mile Range Group||||||
24044|Trooper Creek Formation|22675|6|Mentioned|p13|||||||||
24044|Trooper Creek Formation|22847|5|Briefly described|p 7|||||||||
24044|Trooper Creek Formation|23278|4|Described|p80-2, Fig1p81||Ordovician|||||||
24044|Trooper Creek Formation|23318|4|Described|p392 Fig.1|Early Ordovician|Early Ordovician|Of the Seventy Mile Range Group. Andesitic, dacitic and rhyolitic lavas, intrusions and associated breccia; mudstone, siltstone, sandstone; pumice-lithic breccia; silica ironstone; massive sulphide.||||||07-FEB-07
24044|Trooper Creek Formation|23422|4|Described|p170, p206 Table 6.3|Middle Ordovician|Cambrian|Of Seventy Mile Range Group.  Overlying unit: Rollston Range Formation. Underlying unit: Mount Windsor Volcanics.||||||
24044|Trooper Creek Formation|23430|4|Described|p469-470.|||Of Seventy Mile Creek Group.||||||
24044|Trooper Creek Formation|23431|5|Briefly described|p537|||||||||
24044|Trooper Creek Formation|23504|5|Briefly described|Map Legend|Ordovician|Cambrian|of Seventy Mile Range Group.||||||
24044|Trooper Creek Formation|23505|5|Briefly described|Map legend|Ordovician|Cambrian|of Seventy Mile Range Group.||||||
24044|Trooper Creek Formation|23764|5|Briefly described|p340|Ordovician|Cambrian|Submarine volcanic succession.   Parent: Seventy Mile Range Group.||||||
24044|Trooper Creek Formation|23852|4|Described|p816|Ordovician|Cambrian|Of Seventy Mile Range Group. Overlying Unit Rollston Range Formation. Underlying Unit Mount Windsor Formation.||||||
24044|Trooper Creek Formation|23940|5|Briefly described|p917 Fig. 3|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group.  Formation is Fm. in text.  GeologicalProvince: Mount Windsor subprovince.||||||
24044|Trooper Creek Formation|23950|5|Briefly described|p1134 Fig. 1|Ordovician|Ordovician|Of the Seventy Mile Range Group. Overlies the Mount Windsor Formation.||||||
24044|Trooper Creek Formation|23951|6|Mentioned|p1150|||||||||
24044|Trooper Creek Formation|23952|4|Described|p1176 Fig. 1|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Conformably overlain by the Rollston Range Formation. Geological Province: Mount Windsor subprovince||||||
24044|Trooper Creek Formation|23953|5|Briefly described|p1201, p1202 Fig. 1|Ordovician|Cambrian|Conformably overlain by the Rollston Range Formation. Geological Province: Mount Windsor subprovince||||||
24044|Trooper Creek Formation|23954|5|Briefly described|p1227|||Max. Thickness: 2000m.||||||
24044|Trooper Creek Formation|23988|5|Briefly described|p15|Early Ordovician|Early Ordovician|Of Seventy Mile Range Group.||||||
24044|Trooper Creek Formation|24035|5|Briefly described|p2, p3 Fig. 1, p4, p6 Fig. 3, p7 Fig. 4b|Early Ordovician|Early Ordovician|Of Seventy Mile Range Group. Overlain by the Campaspe Formation. Andesitic and felsic volcanics.||||||
24044|Trooper Creek Formation|24424|5|Briefly described|p524|Early Ordovician|Late Cambrian|Of 70 Mile Group. Geological Province: Lolworth-Ravenswood Province.||||||
24044|Trooper Creek Formation|37765|5|Briefly described|p9|||||||||
24044|Trooper Creek Formation|38658|6|Mentioned|p152|||||||||
24044|Trooper Creek Formation|39445|6|Mentioned|p66|||||||||
24044|Trooper Creek Formation|40746|3|Fully described|p349|||Mention p348.||||||10-FEB-09
24044|Trooper Creek Formation|41675|6|Mentioned|p52|||||||||
24044|Trooper Creek Formation|42279|5|Briefly described|p27|||||||||
24044|Trooper Creek Formation|42398|6|Mentioned|PB2|||||||||
24044|Trooper Creek Formation|42407|5|Briefly described|p34|||||||||
24044|Trooper Creek Formation|42633|4|Described|p15|||||||||
24044|Trooper Creek Formation|43093|5|Briefly described|p14|||of Seventy Mile Range Group||||||
24044|Trooper Creek Formation|43128|5|Briefly described|Fig.6,p476|||||||||
24044|Trooper Creek Formation|43259|6|Mentioned|Appendix 1,p7.|Ordovician|Cambrian|Upper Cambrian - Lower Ordovician in age.||||||03-DEC-13
24044|Trooper Creek Formation|43763|4|Described|p741|Early Ordovician|Cambrian|||||||
24044|Trooper Creek Formation|43773|5|Briefly described|Fig.1,p765|||||||||
24044|Trooper Creek Formation|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
24044|Trooper Creek Formation|43936|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||
24044|Trooper Creek Formation|50153|6|Mentioned|p15|||||||||
24044|Trooper Creek Formation|60659|5|Briefly described|p10|||Intermediate to minor felsic lavas, volcaniclastics, volcanogenic and mass flow deposits. Overlies Mount Windsor Volcanics; unconformably overlain; Pallamana Sandstone of  Drummond Basin, and Rollston Range Formation.||||||07-FEB-11
24044|Trooper Creek Formation|62079|6|Mentioned|p43|Ordovician|Cambrian||||Includes Mount Windsor Volcanics.|||
24044|Trooper Creek Formation|62470|5|Briefly described|p181 Fig. 1|Ordovician|Cambrian|Of Seventy Mile Range Gp.Consists of basaltic to rhyolite lavas, synvolcanic intrusions and associated volcaniclastic rocks as. Overlies Mount Windsor Fm; overlain by Rollston Creek Fm. max. thickness: 4000m.||||||07-FEB-11
24044|Trooper Creek Formation|64850|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Andesitic/basaltic lava; coarse to medium-grained andesitic volcaniclastic sediments; coarse andesitic fragmental rocks.||||||09-FEB-09
24044|Trooper Creek Formation|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Fine- to medium-grained sandstone, siltstone and shale; fossiliferous; and, andesitic/basaltic lava; coarse to medium-grained andesitic volcaniclastic sediments, coarse andesitic fragmental rocks.||||||
24044|Trooper Creek Formation|68731|5|Briefly described|p145, p146|Early Ordovician|Early Ordovician|Graptolites near the base of this unit are diagnostic of a lower Tremadocian age. It includes a diverse facies array of deep marine origin, as well as some lenses which have a shallow marine origin. Minimum age constrained by the Seventy Mile Range Group.|< 485 Ma|Of the Seventy Mile Range Group.|||Comprises intermediate to minor felsic lavas, volcaniclastics, volcanogenic and mass flow deposits locally invaded by small hypabyssal felsic intrusions.|
24044|Trooper Creek Formation|68900|4|Described|p12-p14|Ordovician|Ordovician|Originally defined by Henderson (1986). Crops out on the northern edge of HARVEST HOME and PAJINGO map sheets where it forms low topography. Age assigned on the basis of palaeontological data. Weak to moderate K signature in airborne radiometrics and very low magnetic signature. Deposited in a sub-aqueous, deep water environment proximal to submarine volcanic centres.||Seventy Mile Range Group||Conformably overlies the Mount Windsor Volcanics. Overlain by the Rollston Range Formation. Unconformably overlain by the Pallamana Sandstone.|Intermediate to minor felsic lavas, volcaniclastics, volcanogenic and mass flow deposits.|
24044|Trooper Creek Formation|70740|6|Mentioned|p37|||||||||
24044|Trooper Creek Formation|70749|5|Briefly described|p48|Tremadocian|Tremadocian|Charters Towers Province. Contains lower Tremadocian graptolites.||||Overlies Mount Windsor Volcanics.||
38210|Trooper Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Ordovician|||||||
38210|Trooper Supersuite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
38244|Tuckers Suite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Supersuite.||||||
38244|Tuckers Suite|69593|4|Described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|Tuckers Range, Boori, First Pocket, Igneous Complexes; Camp Oven Mountain Complex?||Gabbro, diorite, biotite-hornblende granodiorite to tonalite, biotite granite and leucogranite, monzodiorite, quartz diorite.|
38244|Tuckers Suite|73029|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||Leichhardt Supersuite|Includes Fence Creek Granodiorite.|||
34676|Tuckers Supersuite|22847|5|Briefly described|p15|||||||||
34676|Tuckers Supersuite|24512|6|Mentioned|p5|||||||||
23057|Tulliegorim Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
23057|Tulliegorim Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
23057|Tulliegorim Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 206.  I-Type.||||||
23057|Tulliegorim Granodiorite|43093|6|Mentioned|Table 5,Table 10.|||see also Tullegorim Granodiorite in Appendix 1.||||||
23057|Tulliegorim Granodiorite|43259|4|Described|Appendix 1,p30.|Early Devonian|Late Silurian|||||||
23057|Tulliegorim Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
36568|Tumoulin granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 242.  I-Type.||||||
26962|Tungi Creek Granodiorite|22845|6|Mentioned|p9,39,42,6,74,82|Triassic|Permian|Intrudes Peters Creek Greenstone.||||||
26962|Tungi Creek Granodiorite|22846|4|Described|p6,45,68,76|Late Triassic|Middle Triassic|||||||
26962|Tungi Creek Granodiorite|23609|4|Described|p7, 9-10.|||Also see Fig 1 p6. I-Type granite. North D'Aguilar Block.||||||
26962|Tungi Creek Granodiorite|23799|5|Briefly described|p115 Fig. 10|Triassic|Permian|Creek is Cr. in text of figure.  Geological Province: D'Aguilar Subprovince.||||||
26962|Tungi Creek Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
26962|Tungi Creek Granodiorite|35101|3|Fully described|p71|||||||||
26962|Tungi Creek Granodiorite|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
26962|Tungi Creek Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
26962|Tungi Creek Granodiorite|39445|5|Briefly described|Table 12|||||||||
26962|Tungi Creek Granodiorite|40051|4|Described|p6|||||||||
26962|Tungi Creek Granodiorite|41272|5|Briefly described|M 1of1 H16|||||||||
26962|Tungi Creek Granodiorite|41917|6|Mentioned|p522|||||||||
26962|Tungi Creek Granodiorite|43008|5|Briefly described|map legend|||||||||
26962|Tungi Creek Granodiorite|43588|6|Mentioned|p31|Late Triassic|Early Triassic|||||||
26962|Tungi Creek Granodiorite|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
26962|Tungi Creek Granodiorite|60077|5|Briefly described|Map legend|Triassic|Permian|Medium to coarse-grained, light-grey granodiorite.||||||
26962|Tungi Creek Granodiorite|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Biotite-hornblende granodiorite; hornblende-biotie granite.||||||
26962|Tungi Creek Granodiorite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
26962|Tungi Creek Granodiorite|68679|5|Briefly described|p327, p330-331, p387, p428-429|||Sunshine Coast hinterland, northern New England Orogen. Geochemically similar to Neurum Complex.|225.7 +/- 6 Ma (K-Ar biotite: Green, 1975).|||Intrudes Amamoor, Cambroon and Booloumba beds, Jimna Phyllite and Peters Creek Greenstone.|Metaluminous, I-type. Fine- to medium-grained, equigranular granite core surrounded by fine- to coarse-grained, subequigranular biotite-hornblende granodiorite. Dioritic xenoliths are abundant in the north.|
73045|Tunnel beds|61392|5|Briefly described|p164 Fig. 1||Early Permian|Of the Wildash Group.||||||07-FEB-11
70391|Turkey Beach Granite|65452|6|Mentioned|p6 Fig.2, p29|Late Triassic|Late Triassic|Geochemistry briefly described.||Toogoolawah Group.||||
70391|Turkey Beach Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Pink medium-grained, equigranular biotite, syenogranite; locally abundant microdiorite enclaves up to 2m long; commonly intruded by basalt and felsic dykes.|
70391|Turkey Beach Granite|68679|5|Briefly described|p431, p433|||von Gnielinski et al. (2004).|||||Pink, medium-grained, equigranular biotite syenogranite; miarolitic; locally abundant microdiorite enclaves; basalt dykes. Includes a dioritic phase that forms small, pod-like bodies and has spectacular net-vein relationships with felsic phases.|
75649|Turn Back Granite|73036|5|Briefly described|Map legend|Early Permian|Early Permian||||||Pale pink, medium-grained, slightly to moderately porphyritic biotite monzogranite to granodiorite; locally with rapakivi texture and traces of allanite; also with scattered mafic inclusions up to c. 1 m across.|
81101|Turrawalla Granodiorite|69594|5|Briefly described|p571 Fig.7.45|Early Cretaceous|Early Cretaceous|Southern Connors Subprovince, Bowen Basin. Geochemistry plot.||||||
24052|Turrets Formation|23032|4|Described|p32|Early Carboniferous|Late Devonian|||||||
24052|Turrets Formation|23424|4|Described|Table 8.1 p337.||Famennian|Age: Late Devonian (Famennian); superposition. Of Bundock Creek Group, Bundock Basin. Overlying Unit Teddy Mount Formation. Maximum Thickness 770 m.||||||
24052|Turrets Formation|23430|5|Briefly described|Plate 14.11||Devonian|Also see p507. Of Bundock Creek Group. Graveyard Creek Subprovince.||||||
24052|Turrets Formation|23431|5|Briefly described|p541|||||||||
24052|Turrets Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Tournaisian|Famennian|Of the Bundock Creek Group. Overlain by the Teddy Mountain Formation. Overlies the Bulgeri Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
24052|Turrets Formation|24613|5|Briefly described|p135|||Interpreted as a regressive phase of a fluviatile-deltaic depositional system prograding from the north (Lang 1993).||||||07-FEB-11
24052|Turrets Formation|24614|5|Briefly described|p191 Fig. 1|||Of the Bundock Creek Group. Geological Province: Broken River Province.||||||07-FEB-11
24052|Turrets Formation|41260|3|Fully described|p85|||Described P175||||||
24052|Turrets Formation|41679|6|Mentioned|Fig.2|||||||||
24052|Turrets Formation|41739|2|Defined|p303|Famennian|Frasnian|||||||
24052|Turrets Formation|41740|6|Mentioned|p222|||||||||
24052|Turrets Formation|42054|6|Mentioned|p273|||||||||
24052|Turrets Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
24052|Turrets Formation|42709|6|Mentioned|map legend|||||||||
24052|Turrets Formation|42933|3|Fully described|p162|||Of Bundock Creek Group.||||||04-FEB-08
24052|Turrets Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group.||||||04-FEB-08
24052|Turrets Formation|43603|5|Briefly described|p9|||||||||
24052|Turrets Formation|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Bundock Creek Group.||||||
24052|Turrets Formation|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group. Coarse-grained feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone and lesser conglomerate reworked tuff||||||
24052|Turrets Formation|65214|6|Mentioned|p280|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
24052|Turrets Formation|67402|4|Described|p239, p245 |Famennian|Famennian|Bundock Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in alluvial plain to deltaic and marginal marine environments. Maximum thickness of 770m.||||Overlies the Bulgeri Formation. Overlain by the Teddy Mount Formation.|Feldspathic to lithofeldspathic sandstone, mudstone with lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68336|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone, and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68341|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Teddy Mount Formation. Conformably underlain by the Bulgeri Formation.|Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone, and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68478|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Teddy Mount Formation. Conformably underlain by the Bulgeri Formation.|Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|68479|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Teddy Mount Formation. Conformably underlain by the Bulgeri Formation.|Coarse-grained, feldspathic to lithofeldspathic (locally volcaniclastic) sandstone, mudstone and lesser conglomerate and reworked tuff.|
24052|Turrets Formation|69030|5|Briefly described|p6|Carboniferous|Devonian|Bundock Basin (Broken River Province).||Bundock Creek Group.||||
24052|Turrets Formation|69592|5|Briefly described|p259, p272 Fig.4.61, p273-274, p276|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. 900-1400m thick in western part of the Basin, thinning eastwards to 100m. The only fossils are plant fragments, mainly calamitacean. Paralic, fluvio-deltaic deposits from the N and W.||Bundock Creek Group.||Conformably overlies Jamieson Member (Bulgeri Formation). Is overlain conformably by Teddy Mount Formation.|A succession of lithofeldspathic to feldspathic sandstone, pebbly sandstone and siltstone with subordinate mudstone, quartzose conglomerate and tuff. Crystal-vitric tuff locally near the base.|
27997|Turtle Swamp Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Lankelly Suite of the Kintore Supersuite. Intrudes Holroyd Group||||||
27997|Turtle Swamp Granite|43596|4|Described|p31, p28 Tb. 3|||Of Lankelly Suite (Kintore Supersuite).  Intrudes  Sugarbag Creek Quartzite. Consists of abundantly porphyritic muscovite-biotite granite with phenocrysts of microcline; sheraed and cut by several quartz veins on northern margin.||||||15-JAN-09
27997|Turtle Swamp Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
23072|Twelve Mile Schist|23420|5|Briefly described|p 144 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
23072|Twelve Mile Schist|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
23072|Twelve Mile Schist|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
23072|Twelve Mile Schist|43596|4|Described|p13, p20 Tb. 1||Proterozoic|Of Yambo Metamorphic Group.  Predominantly sillimanite-biotite-plagioclase-quartz schist and interlayered quartzite; garnet porphyroblasts are common in both schist and quartzite||||||15-JAN-09
23072|Twelve Mile Schist|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Yambo Metamorphic Group||||||24-JAN-05
23072|Twelve Mile Schist|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier.||Yambo Metamorphic Group.|||Sillimanite-quartz(+/- garnet) schist; quartzite, hornblende amphibolite.|
26329|Twiddler Hill Basalt|23507|5|Briefly described|Map Legend|Pleistocene|Pliocene|||||||
26329|Twiddler Hill Basalt|42625|5|Briefly described|Map legend|Pleistocene|Pliocene|Reserved.||||||
26329|Twiddler Hill Basalt|42810|2|Defined|Table 1 P14|Pleistocene|Pliocene|see also p29.||||||20-AUG-08
26329|Twiddler Hill Basalt|60425|6|Mentioned|p42 Tb. 3|Miocene|Miocene|Part of Atherton Basalt grouping.||||||07-FEB-11
27655|Twin Dams Andesite|23291|4|Described|p95 Tb. 3.10|Early Permian|Early Permian|Parent: Namarrong Volcanic Subgroup. Age: 283+/-3Ma. Thickness: Up to 300m. Geological Province: Georgetown Region.||||||08-JUL-15
27655|Twin Dams Andesite|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Kungaree Volcanic Subgroup, Newcastle Range Volcanic Group.||||||
27655|Twin Dams Andesite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V14.||||||
27655|Twin Dams Andesite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|Of Namarrong Volcanic Subgroup||||||08-OCT-04
27655|Twin Dams Andesite|40542|6|Mentioned|p97|||||||||
27655|Twin Dams Andesite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Namarrong Volcanic Subgroup.||||||
27655|Twin Dams Andesite|43740|5|Briefly described|p10|||Of Namarrong Volcanic Subgroup||||||08-OCT-04
27655|Twin Dams Andesite|50198|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Nammarong Volcanic Subgroup. [misspelling of Namarrong]||||||28-MAY-15
27655|Twin Dams Andesite|68354|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Min age: Early Permian?||Unit in Nammarong Volcanic Subgroup [misspelling of Namarrong].|||Grey to green aphyric augite-pigeonite basaltic andesite.|08-JUL-15
36653|Twin Humps Granite|23420|5|Briefly described|p 130|||Also see Twin Humps Adamellite. Of Weymouth Supersuite.||||||
36653|Twin Humps Granite|69593|5|Briefly described|p512|||Jardine Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|285 Ma.||||I-type.|
36653|Twin Humps Granite|71031|6|Mentioned|p15, p20|Early Permian|Early Permian||285 +/- 9 Ma (SHRIMP, Black et al, 1992a,b)|||||
36653|Twin Humps Granite|71792|6|Mentioned|p25|||Outcrops north-northwest of Coen.|c. 285 +/- 9 Ma (Black et al, 1992a & b)|||||
36653|Twin Humps Granite|71849|3|Fully described|p1, p4-5, p8, p12, p36, p79, p102, p108|Permian|Permian|See also p2, p6, p11, p126-132, p144, p179-183, p186-187, p195. Formerly the Twin Humps Adamellite of Willmott et al. (1973) and Whitaker and Gibson (1977). Cape York Peninsula Batholith. Two discrete plutons, detailed. Geophysics described; lithologies and geochemistry in some detail. Early Permian; discrepancy with earlier age determinations discussed. Some potential for small vein and greisen deposits.|285 +/- 9 Ma (SHRIMP; Black et al., 1992).|Weymouth Supersuite.||Intrudes Coen Metamorphic Group, McIlwraith and Lankelly Granites.|Reduced I-type. Heterogeneous unit. White to pale pink, medium-grained, moderately porphyritic hornblende-biotite to biotite monzogranites, leucocratic biotite monzogranite.|10-APR-19
36653|Twin Humps Granite|71854|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||White to pale pink, pale pinkish-grey, or pale brown, medium-grained, moderately porphyritic hornblende-biotite monzogranite to biotite monzogranite, and more even-grained leucocratic biotite monzogranite.|
36653|Twin Humps Granite|72983|6|Mentioned|p60|||Ages from Black et al. (1992). Age is within uncertainty of that of Weymouth Granite and Wolverton Granite.|285 +/- 9 Ma|Weymouth Supersuite||||
34988|Twins basalt|22941|6|Mentioned|p292 fig4|||||||||
30106|Two Creek Granodiorite|22847|3|Fully described|p 45|Ordovician|Early Ordovician|||||||
30106|Two Creek Granodiorite|23422|5|Briefly described|p173, p210 Table 6.6|Middle Ordovician|Middle Ordovician|Of Columbia Creek Supersuite.||||||
30106|Two Creek Granodiorite|23430|5|Briefly described|p480|||Ravenswood Batholith Province.||||||
30106|Two Creek Granodiorite|23504|5|Briefly described|Map Legend||Ordovician|||||||
30106|Two Creek Granodiorite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Early to Middle Ordovician||||||18-JUL-14
30106|Two Creek Granodiorite|43259|4|Described|Appendix 1,p30.||Ordovician|Ordovician?.||||||
30106|Two Creek Granodiorite|43936|5|Briefly described|Map Legend||Ordovician|||||||
30106|Two Creek Granodiorite|68731|6|Mentioned|p147|||Rienks, Tenison, Woods, and Wyborn (1995). Has similar geochemistry and setting to the Columbia Creek Complex.||||||
26186|Two Mile Granite|22847|3|Fully described|p 50|Early Devonian|Late Silurian|||||||
26186|Two Mile Granite|23422|5|Briefly described|p213 Table 6.8|||||||||
26186|Two Mile Granite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26186|Two Mile Granite|42245|2|Defined|p39|Early Devonian|Late Silurian|Reserved as Two Mile Adamellite||||||
26186|Two Mile Granite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
26186|Two Mile Granite|43259|4|Described|Appendix 1,p24.|Early Devonian|Late Silurian|Late Silurian - Early Devonian?. Possibly related to Heathfield West Tonalite & Emu Mill Granodiorite||||||03-DEC-13
26186|Two Mile Granite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26186|Two Mile Granite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
26186|Two Mile Granite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Two Mile grt.||Unit in Millchester Supersuite.||||
25561|Two Rail Monzogranite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
25561|Two Rail Monzogranite|22781|4|Described|p29|Paleozoic|Paleozoic|Flyspeck Supersuite||||||07-NOV-08
25561|Two Rail Monzogranite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Flyspeck Granodiorite and Glen Garland Granodiorite.||||||
25561|Two Rail Monzogranite|42610|2|Defined|p26|Early Devonian|Early Devonian|Age assumed similar to Glen Garland Granodiorite - 398Ma. Res. as Two Rail.||||||10-DEC-19
25561|Two Rail Monzogranite|43738|6|Mentioned|Fig.12,p38|||||||||
25561|Two Rail Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
25561|Two Rail Monzogranite|71031|6|Mentioned|p26, p33|||||||(Probably) intrudes the Flyspeck Granodiorite.||
25561|Two Rail Monzogranite|71849|6|Mentioned|p8, p120, p195|Devonian|Devonian|Significance of allanite-epidote association discussed.||Flyspeck Supersuite.||||
25561|Two Rail Monzogranite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Flyspeck Supersuite.|||Pale grey, sparsely and weakly porphyritic, allanite-biotite monzogranite grading to granite and granodiorite, porphyritic in part.|
23078|Tynemouth Diorite|42980|5|Briefly described|Fig.5,p305|||||||||
28038|Ukin Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group, Edward River Metamorphic Group||||||
28038|Ukin Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p35|||Of Ebagoola Suite (Kintore Supersuite). Intrudes Astrea Formation.  Pale grey to cream sparsely porphyritic muscovite-biotite granite; pegmatite.||||||27-JAN-09
28038|Ukin Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
70397|Ulangool Granite|65452|6|Mentioned|p6 Fig.2|Late Triassic|Late Triassic|||||||
70397|Ulangool Granite|67203|6|Mentioned|p6|Triassic|Triassic|||||||
70397|Ulangool Granite|68319|5|Briefly described|Map Legend|Late Triassic|Late Triassic||||||Medium to very coarse-grained porphyritic biotite granite; common rhyolite and dacite dykes; locally weakly foliated.|
70397|Ulangool Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Medium to very coarse-grained porphyritic biotite granite; common rhyolite and dacite dykes; locally weakly foliated.|
70397|Ulangool Granite|68679|5|Briefly described|p433|Late Triassic|Late Triassic|Bundaberg-Agnes Water-Biloela region.|||||Medium- to coarse-grained porphyritic biotite granite; rhyolite and dacite dykes; weak foliation.|
70397|Ulangool Granite|73450|6|Mentioned|p16|||||||||
39593|Umbrella Granodiorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
39593|Umbrella Granodiorite|50317|5|Briefly described|Map Legend|Triassic|Permian|Of the Bouldercombe Igneous Complex. Pale grey medium-grained biotite-hornblende granodiorite.||||||28-MAY-04
39593|Umbrella Granodiorite|68008|3|Fully described|p225, p248, p334-335, p341, p343|Early Triassic|Permian|See also p346-350, p352, p381, p620. Defined in this study. Previously the northern tonalite phase of the Westwood Complex of Wood (1974). 12 x 4km intrusive. Named after Umbrella Creek. Typical exposures form low ridges on both sides of Junction Creek 10km ENE of Westwood. Other exposures listed. Geochemistry described: similar to Rocky Point Granodiorite. Geophysics modelling.|243 +/- 5 Ma (K-Ar biotite).|Bouldercombe Igneous Complex.||Is overlain nonconformably by Bushley Dacite. Intrudes Flaggy Quartz Monzodiorite. Is intruded by Moonkan Granite.|Pale grey, medium-grained, massive biotite-hornblende granodiorite with ubiquitous, and locally abundant, inclusions of darker grey and finer-grained material.|
41352|Undercliffe Falls Monzogranite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Moonbi Suite.  Previously known as Bungulla Porphyritic Adamellite.||||||
41352|Undercliffe Falls Monzogranite|61790|6|Mentioned|p318, p319, p320|||Not intended as a formal name, more of a petrology descriptor, phase of Undercliffe Falls Adamellite.||||||27-OCT-08
41352|Undercliffe Falls Monzogranite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Greyish pink to pinkish grey, mediuym- to fine-grained (groundmass), coarsely porphyritic titanite-hornblende-biotite monzogranite to granodiorite; with pink K-feldspar megacrysts; mafic enclaves common; high magnetic response.||||||30-JAN-09
41352|Undercliffe Falls Monzogranite|68111|5|Briefly described|p969 Tb.1|Anisian|Anisian||ca 245, Rb-Sr (biotite) (Shaw 1994).|Of the Stanthorpe Supersuite.||||
41352|Undercliffe Falls Monzogranite|69639|5|Briefly described|p80, p157, p192, p222|||New England Orogen. Considered to be identical to the Bungulla Monzogranite and geochemically similar to the Bookookoorara Monzogranite. In contact with the Cullendore Granite, although the relationship between the two is unclear.||||||
41352|Undercliffe Falls Monzogranite|71628|4|Described|p7: 1; p11: 1-2, 5, 7, 9, 12, 14, 24|||See also p11: 35-46; p15: 1, 32-33, 37-38, 40, 52-54, 56-57, 59, 68-69, 115-116; p16: 1-4, 6-14, 16, 18-20, 22; p19: 80-83, 87, 102. Barnes (1987). Included in the Moonbi Plutonic Suite by Shaw and Flood (1981). Referred to more recently by NSWGS (e.g. Henley et al., 2001) as Bungulla Monzogranite. Named after a local geographic feature. Comprises two masses, Undercliffe Falls and Boorook (described). Forms whalebacks and tors in gently undulating hills. Geochemistry described; similar to Bungulla Monzogranite. RELATED UNITS (continued): Is intruded by Mount Lindesay and Jenners Monzogranites (Stanthorpe Complex) and Cullendore Syenogranite. Abuts Stanthorpe Complex.|245.4 Ma (Rb-Sr biotite: Shaw and Flood, 1993).|Bungulla Suite.||Intrudes and is faulted against Drake Volcanics and Razorback Creek Mudstone. May intrude The Ridge Monzogranite. Has a complex boundary with Karonstadt Complex (detailed). See COMMENTS for more.|Medium- to coarse-grained, strongly porphyritic biotite-hornblende granodiorite-monzogranite characterised by abundant pink, and locally white, K-feldspar phenocrysts, enclaves and megascopic titanite. Described in great detail. I-type.|
31115|Upland Granodiorite|23032|4|Described|p40,41||Early Devonian|K/Ar Ages: 407Ma & 390Ma.||||||
31115|Upland Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
31115|Upland Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
31115|Upland Granodiorite|43480|2|Defined|7-34|Devonian|Silurian|Age: 407Ma||||||
31115|Upland Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey, pinkish-grey, porphyritic muscovite-biotite granodiorite with common alkali phenocrysts to 4 cm.|
31115|Upland Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Foliated, grey pinkish-grey, porphyritic muscovite-biotite granodiorite with common alkali phenocrysts to 4 cm.|
31115|Upland Granodiorite|69592|5|Briefly described|p281, p284-285|||Reedy Springs Batholith, Charters Towers Province. Geochemistry plots.||Upland Supersuite.|||I-type.|
77823|Upland Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Charters Towers Province. This unit; the Barrabas, Brittania, Craigie, Deane, Millchester and Toms Hole Supersuites; the Amarra, Broughton River, Grasstree and Hodgon Suites; Hungerford Granite; and various ungrouped Siluro-Devonian plutonic units, are all mapped under the same symbol, SDg.||||||
77823|Upland Supersuite|69592|4|Described|p280-281, p283-284, p289 Fig.4.88|||Rienks (1997). Reedy Springs Batholith, NW Charters Towers Province. Geochemistry described; very similar to the White Springs Supersuite. CONSTITUENTS continued: Bombarri Creek complex; Glenloth, Reillys Gully, Stawell granites.|410 +/- 6 Ma (SHRIMP: Withnall and Hutton, 1997).||Baby, Big Bore, Blanders, Bombarri, Bubbling, Capel, Cargoon, Cracknell, Hogg, Milky, Mistake, Newburgh, Strathtay, Upland, Woongalee, Yering Granodiorites; Thursday Monzogranite. More in COMMENTS.|Intrudes Cape River Metamorphics.|Biotite granodiorite, muscovite-biotite granodiorite to monzogranite; accessory titanite, allanite, epidote, zircon. I-type.|
77823|Upland Supersuite|71849|6|Mentioned|p173-176|Devonian|Silurian|Reedy Springs Batholith. Geochemistry discussed in contrast with Flyspeck and Blue Mountains Supersuites.|||||I-type granitoids.|
75727|Upper Rosetta Creek Granite|70740|5|Briefly described|p122, p129, p130|Permian|Carboniferous|Outcrop characteristics and distribution briefly discussed. Appears to intrude the Bluestone Creek Granodiorite and units of the Bulgonunna Volcanic Group.|||||Coarsely porphyritic, biotite microgranite to microsyenogranite. Fine to medium-grained moderately porphyritic leucocratic biotite monzogranite that is commonly granophyric also occurs.|05-OCT-17
35092|Urannah Suite|23042|5|Briefly described|p9||Late Carboniferous|Probable misspelling of Urannah Complex.||||||
35092|Urannah Suite|23162|4|Described|p876, 877||Late Carboniferous|New term to encompass the chemically related plutons and felsic dykes of the Urannah batholith, plus its outliers. Age: Zircon SHRIMP 308.2+/-7.1Ma & 304.3+/-5.8Ma.||||||
35092|Urannah Suite|60298|6|Mentioned|p192|||Plutonic. QLD. Geological Province: New England Orogen.||||||17-DEC-07
35092|Urannah Suite|60659|5|Briefly described|p19|||Includes Late Carboniferous and Early Permian granitoids.||||||07-FEB-11
35092|Urannah Suite|61035|4|Described|p11|Late Carboniferous|Late Carboniferous|Of the Urannah Batholith. Age: ~308Ma and ~304Ma (Allen et al, 1998). Geological Province: Connors Sudprovince.||||||07-FEB-11
35092|Urannah Suite|61784|5|Briefly described|p297|Permian|Carboniferous|Age: ~280Ma. Within the Urannah Batholith.||||||
35092|Urannah Suite|68679|6|Mentioned|p363, p366-368|||Allen et al. (1998); one of their three Suites comprising the Carboniferous-early Permian Urannah Batholith. Geochemistry summarised with plots.|||||I-type.|
35092|Urannah Suite|70329|5|Briefly described|p3 Fig.3|Permian|Carboniferous|Northernmost New England Orogen. Batholith (Connors Arch), associated with late-stage dykes: felsic ~284 Ma, and mafic 273-229 Ma.|308-284 Ma (Allen et al., 1998).||||Includes felsic and mafic dykes.|
35092|Urannah Suite|73197|6|Mentioned|p471|Guadalupian|Late Carboniferous|New England Orogen, northern. Connors Subprovince. Most plutons are contemporaneous with rifting, predominantly I-type. Referred to as Urranah Batholith on p470, p472 Tb.2? Urranah Batholith has U-Pb zircon ages of 305.7 +/- 1.7 Ma, 286.7 +/- 5.2 Ma sourced from Allen et al., (1998), Cross et al., (2012b), Cross et al., (2012a), Withnall et al., (2009). The 286.7 Ma age is corrected from 283.9 +/- 5.2 Ma for using the SL13 standard, unclear which reference this is from.|||||Granitoids.|
36466|Urannah Supersuite|23549|5|Briefly described|p527|||Intruded by the Thunderbolt Supersuite.  In the Connors Arch (central Queensland).  See also p516 Fig. 1.||||||05-APR-05
24057|Urdera Granodiorite|22847|3|Fully described|p 49|||||||||
24057|Urdera Granodiorite|23422|5|Briefly described|p213 Table 6.8|||||||||
24057|Urdera Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 460. I-Type.||||||
24057|Urdera Granodiorite|42633|5|Briefly described|Table 1 P8|||Reserved.||||||
24057|Urdera Granodiorite|42750|2|Defined|p42|Early Devonian|Late Silurian|||||||
24057|Urdera Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Silurian|Middle Silurian to Early Devonian age.||||||
24057|Urdera Granodiorite|43259|4|Described|Appendix 1,p49.|Early Devonian|Late Silurian|||||||
24057|Urdera Granodiorite|43933|5|Briefly described|Map Legend|Devonian|Silurian|||||||
24057|Urdera Granodiorite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
24057|Urdera Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Urdera gdrt.||Unit in Millchester Supersuite.||||
24057|Urdera Granodiorite|62521|5|Briefly described|p23-24, p55|Early Devonian|Late Silurian|Of Millchester Creek Supersuite. Geological Province: Ravenswood Batholith. See also p18.||||||14-JAN-08
24057|Urdera Granodiorite|68576|6|Mentioned|Q_11: p42|||Charters Towers.||||||
41941|Uruba Granite|23042|5|Briefly described|Fig 2||Carboniferous|||||||
41941|Uruba Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
41941|Uruba Granite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Fine- to medium-grained leucocratic biotite granite and microgranite with common aplite and pegmatite; porphyritic hornblende microdiorite and medium-grained biotite hornblende granodiorite; microdiorite dykes. Part of the Urannah Batholith.||||||16-MAR-06
41941|Uruba Granite|65388|2|Defined|p388-389, 135, 362, 364, 365, 380, 388|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. May intrude Teemburra Igneous Complex. Probably intruded by Morugo Granite. May be younger than Pisgah Igneous Complex, Gargett Granodiorite. Postulated age given. Most common rock type is pale pink, medium to coarse-grained equigranular biotite granite, sheared in places.||||||
69841|Valdora Dacite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
69841|Valdora Dacite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Dacite.|
69841|Valdora Dacite|73450|6|Mentioned|p84|Triassic|Triassic|[Probably a variation on Valdora Dacite].||||||
36546|Valley Creek complex|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 209.||||||
36307|Van Lee Granite|23291|5|Briefly described|p35|||Probably part of the White Springs Supersuite. See also Van Lee granite. Geological Province: Georgetown Region.||||||08-JUL-15
36307|Van Lee Granite|23510|5|Briefly described|Map Legend||Silurian|of White Springs Supersuite.||||||
36307|Van Lee Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
80681|Vardon Granite|71849|3|Fully described|p2, p8, p15, p57-58, p60, p84, p87-90|Devonian|Devonian|See also p150, p155-157, p159, p195. New name, after the Parish of Vardon. Previously mapped as part of Kintore Adamellite by Willmott et al. (1973). Included in Ebagoola Suite by Mackenzie and Knutson (1992). Narrow NW-trending belt ~14km long and up to ~3km wide, c.16km SW of Coen. Type area is around MGA 720808 8453508 on Lochinvar station. Poorly exposed; isolated boulders. Geophysics briefly described; lithology and geochemistry described. Not isotopically dated. ?Pre-dates Tadpole Granite; post-dates Whites Creek Granodiorite.||Ebagoola Suite.||Adjacent to and intrudes Whites Creek Granodiorite.|Deformed and recrystallised, megacrystic, two-mica granite with scattered, irregular, highly porphyritic zones containing locally abundant K-feldspar to ~15cm long. Minor to trace garnet, rare sillimanite and altered cordierite. S-type.|
80681|Vardon Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Ebagoola Suite.|||Pale grey, medium-grained, slightly to highly and coarsely porphyritic (garnet-)biotite-muscovite granite; irregularly distributed K-feldspar megacrysts to ~15cm; extensively deformed and recrystallised.|
34946|Variegated Limestone|22954|6|Mentioned|p18|||(Jones et al. 1971).||||||
24550|Venetia Formation|23032|4|Described|p17,34|Carboniferous|Tournaisian|||||||
24550|Venetia Formation|23424|4|Described|Table 8.1 Fig 8.4 p338.|Early Carboniferous|Late Devonian|Age: Latest Devonian to early Carboniferous (latest Fammenian to Tournaisian); conodonts and brachiopods faulted against the Graveyard Creek Group. Of Clarke River Group, Clarke River Basin. Maximum thickness 500 m.||||||21-JUN-13
24550|Venetia Formation|23430|4|Described|Plate 14.11 + p508|||Laterial equivalent to Ruxton Formation.  Of Clarke River Group.  Camel Creek Subprovince. Clarke River Basin Province.||||||
24550|Venetia Formation|23431|5|Briefly described|p542|||Of Clarke River Group.||||||
24550|Venetia Formation|23619|5|Briefly described|p33 Table 1||Carboniferous|Clarke River Basin Province.||||||
24550|Venetia Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Tournaisian|Tournaisian|Of the Clarke River Group. Overlain by the Lyall Formation. Formation is Fmn in text. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
24550|Venetia Formation|24613|5|Briefly described|p77, p135|Late Devonian|Late Devonian|Of the Clarke River Group. Geological province: Clarke River Basin.||||||07-FEB-11
24550|Venetia Formation|24614|4|Described|p191 Fig. 1, p202|Tournaisian|Tournaisian|Lower section of the Clarke River Group. Thickness: 230m. Geological Province: Clarke River Basin.||||||07-FEB-11
24550|Venetia Formation|40943|2|Defined|p52|Tournaisian|Tournaisian|It may range from latest to Late Visean Prob. Tournaisian. See also misspelling Venetian Formation.||||||
24550|Venetia Formation|40954|6|Mentioned|p132|||||||||
24550|Venetia Formation|41260|3|Fully described|p23|||||||||
24550|Venetia Formation|41776|4|Described|p527|||||||||
24550|Venetia Formation|41823|5|Briefly described|p161|||||||||
24550|Venetia Formation|41824|6|Mentioned|p201|||||||||
24550|Venetia Formation|42692|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
24550|Venetia Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
24550|Venetia Formation|42933|3|Fully described|p203|||Of Clarke River Group.||||||04-FEB-08
24550|Venetia Formation|43113|5|Briefly described|Table 1 p20|||||||||
24550|Venetia Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Clarke River Group.||||||
24550|Venetia Formation|67402|4|Described|p239, p244, p245 fig BND/CLR3|Tournaisian|Famennian|Clarke River Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under alluvial fan, alluvial plain or shelf conditions. Maximum thickness of 500m.||Clarke River Group||Equivalent to the Ruxton Formation. Overlain by the Lyall Formation.|Quartzose to feldspathic sandstone and conglomerate, siltstone, mudstone, local calcareous sandstone and limestone, minor tuffaceous siltstone.|
24550|Venetia Formation|67848|6|Mentioned|p5 Fig.3, p15 Fig.12.|Early Carboniferous|Early Carboniferous|Greenvale Province [?].||||||03-APR-17
24550|Venetia Formation|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone.|
24550|Venetia Formation|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone; polymictic pebble to boulder conglomerate (mapped separately).|
24550|Venetia Formation|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone; polymictic pebble to boulder conglomerate (mapped separately).|
24550|Venetia Formation|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone.|
24550|Venetia Formation|68478|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Of the Clarke River Group.||Conformably overlain by the Lyall Formation.|Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone.|
24550|Venetia Formation|68479|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Of the Clarke River Group.||Conformably overlain by the Lyall Formation.|Quartzose to feldspathic sandstone and conglomerate, siltstone and mudstone; local fine-grained calcareous sandstone and impure limestone with marine fossils; minor tuffaceous siltstone.|
24550|Venetia Formation|68576|6|Mentioned|Q_11: p34-35, p38|||Greenvale area.||||||
24550|Venetia Formation|69030|5|Briefly described|p6, p17|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province. Hosts gold  mineralisation. Alluvial to shallow-marine sediments.||Clarke River Group.||||
24550|Venetia Formation|69079|6|Mentioned|p66|||Several anomalous zones of gold mineralisation in quartz veining were investigated in the Clarke River Basin; drilling encountered no major mineralised zone.||||||
24550|Venetia Formation|69592|5|Briefly described|p252, p274 Fig.4.65, p275, p279|Tournaisian|Tournaisian|Clarke River Basin. Up to 500m thick. Age from fossils including sporadic Leptophloem stem and trunk moulds, marine macrofossils and conodonts. Overlaps in age with Ruxton Formation.||Clarke River Group.||Is overlain conformably by Lyall Formation.|Mainly coarse-grained lithofeldspathic sandstone, pebbly sandstone and conglomerate with subordinate siltstone and tuff; basal pebble to boulder conglomerate overlain by  calcareous siltstone, sandstone, impure limestone and shelly conglomerate.|
24550|Venetia Formation|73201|6|Mentioned|p613|Carboniferous|Late Devonian|||||||
39645|Vera-Nancy Volcanics|60659|4|Described|p12-13, p49|||Informally divided into Mount Janet Volcanics (andesitic) and Mount Starlight Formation (dacitic to rhyolitic). Geological Province: Drummond Basin. See also p50-51 Figs. 2,3.||||||07-FEB-11
39645|Vera-Nancy Volcanics|62074|5|Briefly described|p3|||Hosts the Pajingo gold mineralisation.||||Overlies Palamana Sandstone.|Andesitic to rhyolitic.|11-AUG-15
39645|Vera-Nancy Volcanics|64850|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Rhyolitic and andesitic lava, rhyolitic ignimbrite; minor volcaniclastic sandstone. Two subunits comprise: rhyolitic lava and ignimbrite with minor volcaniclastic sandstone; and andesitic lava.||||||
39645|Vera-Nancy Volcanics|64852|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Rhyolitic and andesitic lava, rhyolitic ignimbrite; minor volcaniclastic sandstone; and an unnamed subunits of rhyolitic lava/ignimbrite with minor volcaniclastic sandstone.||||||10-FEB-09
39645|Vera-Nancy Volcanics|68731|6|Mentioned|p193|||||||Underlain by the Pallamana Sandstone.||
39645|Vera-Nancy Volcanics|68900|2|Defined|p1, p37-p38, p47-p49|||Drummond Basin. Primarily restricted to PAJINGO extending a short distance into HARVEST HOME map sheet. Hosts the Vera-Nancy epithermal gold mineralisation system. Generally produces hilly topography that includes Mount Janet and Mount Ross. A type area is proposed with its north-eastern corner at GR 449000 7730000 and south-western corner at GR 440000 77260000 in HARVEST HOME. Appears to have a low radiometric signature in all channels and produces a moderately strong magnetic response. Andesite is the major host to gold mineralisation. interpreted to have been deposited in a subaerial, terrestrial environment. Thickness is unknown due to a lack of continuous sections. Potential age equivalent to the Silver Hills Volcanics.||||Overlies the Pallamana Sandstone.|Andesitic, dacitic and rhyolitic lavas, rhyolitic ignimbrite and volcanolithic sandstone.|
23106|Verdure Andesite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
23106|Verdure Andesite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
23106|Verdure Andesite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V128.||||||
23106|Verdure Andesite|23616|5|Briefly described|Table 3 p48|||Of Boonmoo Volcanic Subgroup||||||
23106|Verdure Andesite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
23106|Verdure Andesite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|of Boonmoo Volcanic Subgroup.||||||
23106|Verdure Andesite|43567|5|Briefly described|Table 2,p400|||||||||
23106|Verdure Andesite|43626|2|Defined|p27||Late Carboniferous|between 306+/-3 Ma and 304+/-4 Ma||||||
23106|Verdure Andesite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
23106|Verdure Andesite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
23106|Verdure Andesite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Boonmoo Volcanic Subgroup.|||Very dark grey, welded, lithics-poor, crystal-rich to very crystal-rich, orthopyroxene?-hornblende-augite andesitic ignimbrite; minor highly porphyritic, andesitic lava; rare fine-grained lapilli tuff.|
83681|Vermont Seam, Lower|73305|6|Mentioned|p553 Fig.5, p556 Tb.3, p559|Late Permian|Late Permian|Northern Bowen Basin. Coal seam in the Burngrove Formation, 1 to 5 m thick, split from the Upper Vermont Seam by the Yarrabee Tuff. Mostly associated with the overlying Yarrabee Tuff except for a localised area merged with the underlying Girrah Seam.||Burngrove Formation|||Coal seam.|
83682|Vermont Seam, Upper|73305|6|Mentioned|p560|Late Permian|Late Permian|Northern Bowen Basin. Split from the Lower Vermont Seam by the Yarrabee Tuff. Locally merges with the Leichhardt Seam.||Rangal Coal Measures||||
75640|Viola Creek Granodiorite|73036|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Grey, fine to medium-grained, slightly porphyritic biotite-hornblende granodiorite; strongly foliated, with traces of titanite; minor finer grained, strongly foliated biotite granite.|
32048|Voewood Granite|24491|5|Briefly described|p22|||Previously included as part of Galloway Plains Tonalite.||||||
32048|Voewood Granite|24615|5|Briefly described|CD|Triassic|Triassic|[Rgav].  Pale pink to grey, medium-grained biotite granite, locally with pyrite along joint planes.||||||
32048|Voewood Granite|50197|5|Briefly described|Map Legend|Triassic|Triassic|Of the Galloway Plains Igneous Complex.||||||
32048|Voewood Granite|68008|2|Defined|p332, p334, p339, p373-375, p380, p383|Late Triassic|Middle Triassic|See also p389-390, p528-529, p630. New name, after the property Voewood; the type area is a hill W of Lost Spring Creek, 2km ESE of the homestead. The intrusion covers an area 7.5 x 2km, 45km NE of Biloela. Forms undulating hills, topographically higher than surrounding Bocoolima Granodiorite. Geophysics described and modelled; contrasted with Bocoolima Granodiorite. Geochemistry described.|233.6 +/- 6.8 Ma (U-Pb zircon; Fanning, 2012).|Galloway Plains Igneous Complex.||Intrudes (and is completely surrounded by) Bocoolima Granodiorite.|Uniform composition: pale pinkish-grey, medium-grained biotite granite; local muscovite granite. Plagioclase is the dominant mineral (35-50%). [Granite?]. Has closely spaced joints filled with pyrite-bearing quartz veins in the western part.|
32048|Voewood Granite|68679|4|Described|p425, p427, p431|Late Triassic|Late Triassic|A 7.5 x 2 km intrusion in the Galloway Plains Igneous Complex, Yarrol Province. Geochemistry briefly described. This ~233 Ma age comes from two populations at c.240 Ma and c.215 Ma.|233.6 +/- 6.8 Ma (SHRIMP: Fanning, 2012).|Galloway Plains Igneous Complex.||Intrudes and is surrounded by Bocoolima Granodiorite.|Uniform medium-grained biotite granite with possible primary muscovite and local myrmekite.|
32048|Voewood Granite|71592|5|Briefly described|Appendix A.||||234+/-6.8 Ma (SHRIMP U-Pb zircon).||||Granite.|
29323|Wabaredory Granite|23423|6|Mentioned|p239|||||||||
29323|Wabaredory Granite|23713|5|Briefly described|p75 Appendix 2|||See also p22.||||||
29323|Wabaredory Granite|43087|2|Defined|p100|Late Carboniferous||Supersedes Wabadori Granite?||||||
29323|Wabaredory Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Medium-dark green-grey, very strongly porphyritic hornbklende-biotite microgranite.||||||15-JUN-06
29323|Wabaredory Granite|43254|5|Briefly described|map legend||Late Carboniferous|||||||
29323|Wabaredory Granite|43259|4|Described|Appendix 1,p51.|Permian|Carboniferous|||||||
29323|Wabaredory Granite|43285|5|Briefly described|Map Legend||Late Carboniferous|||||||
29323|Wabaredory Granite|43625|6|Mentioned|p49,62|||||||||
29323|Wabaredory Granite|50316|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite? Geological Province: Kennedy Province. Medium to dark greenish grey, fine to medium-grained, highly porphyritic hornblende-biotite granite; moderately to extensively altered.||||||31-MAY-04
29323|Wabaredory Granite|60425|4|Described|p49 Tb.3, p72, p280-1 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite. Age: 308+/-4Ma. (Rb-Sr). Cut into Nightflower Dacite (Featherbed Volcanic Group). I-type. Medium to dark greenish grey, fine- to medium-grained, highly porphyritic hornblende-biotite granite; moderately to extensively altered.||||||07-FEB-11
24551|Waddy Point Volcanics|39445|5|Briefly described|Table 14|||||||||
24551|Waddy Point Volcanics|41265|6|Mentioned|Map legend|Oligocene||||||||
24551|Waddy Point Volcanics|43059|4|Described|p14, Table 2|||||||||
24551|Waddy Point Volcanics|61155|5|Briefly described|p20|Early Oligocene|Early Oligocene|Age: 33-31.5Ma. In the Bundaberg-Maryborough region. ||||||
24551|Waddy Point Volcanics|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran, Gin Gin and Mount Runsome Basalts; Main Range, Minerva Hills and Peak Range Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
24551|Waddy Point Volcanics|68576|5|Briefly described|Q_8B: p22|Neogene|Paleogene|Bedrock on Fraser Island; crops out at Indian Head, Middle Rocks and Waddy Point. Age is given as Tertiary.|||||Trachyte flows and agglomerate, with basalt dykes.|23-OCT-19
79790|Waihora Volcanics|71864|4|Described|p4, p8, p10, p18, p20|||Intersected in GSQ Eulo 2 borehole between 51-135.5 m depth. Conglomerate is matrix supported bordering on clast supported. Clasts are maroon ignimbrite and green porphyritic dacite. These rocks form the basement of the area and are named after Waihora Station on which GSQ Eulo 2 is sited.  Gamma log characteristics and magnetic susceptibility is provided.||||Overlain by the Wallumbilla Formation.|Polymict volcaniclastic conglomerate with boulders and greenish-grey to dark grey, very crystal-rich, strongly welded dacitic ignimbrite that is commonly altered.|
79790|Waihora Volcanics|71965|5|Briefly described|p896,898-899,906,908-909,913-914||Devonian|Geological province: Thomson Orogen. Observed as an irregular moderately magnetic domain cutting across regional trends. Intersected in stratigraphic hole GSQ Eulo 2. Relatively underformed, and shown carbonate alteration and abundant pyrite. Presence of woody plant fragments in the conglomerate indicate a Devonian or younger age.||||Possible volcanic correlative to Currawinya Granite, or Gumbardo Formation.|Polymict volcaniclastic boulder conglomerate overlying a very crystal-rich, strongly welded dacitic ignimbrite.|
79790|Waihora Volcanics|71966|6|Mentioned|p990|Devonian|Devonian|Geological province: southern Thomson Orogen.||||||
35140|Waitara Granite|23042|5|Briefly described|p76, Fig 2|Early Permian|Late Carboniferous|||||||
35140|Waitara Granite|60445|5|Briefly described|p35, p36|||Intrudes Leura Volcanics.||||||
35140|Waitara Granite|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Pinkish grey, fine to medium grained, porphyritic biotite hornblende monzonite to monzogranite with plagioclase and hornblende phenocrysts.||||||
35140|Waitara Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35140|Waitara Granite|65388|2|Defined|p390-391, p121, 135 Fig. 53, p362|Early Permian|Early Permian|Post-Early Permian intrusion. Hornfelses Mount Benmore Volcanics. May intrude Leura Volcanics. Age uncertain, but probably Permian. Pinkish-grey, fine to medium-grained, porphyritic biotite-hornblende monzonite to granite. Some porphyry copper mineralisation adjacent.||||||09-SEP-14
35140|Waitara Granite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Connors Subprovince. This unit, as well as the Camp Creek, Dacey, Olympus,Toobier and Tooloombah Creek Granites; the Bora Creek and Clement Creek Quartz Monzodiorites; and the Sambo Quartz Monzonite, are all mapped under the same symbol, Cgc.||||||
35140|Waitara Granite|68679|6|Mentioned|p347|Carboniferous|Carboniferous|Northern New England Orogen.||||||
23117|Wakara Volcanic Subgroup|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
23117|Wakara Volcanic Subgroup|23423|4|Described|p305 Table 7.3||Early Permian|Age: 278 +/-Ma (Rb-Sr). Featherbed Volcanic Group.||||||
23117|Wakara Volcanic Subgroup|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group.||||||
23117|Wakara Volcanic Subgroup|23501|6|Mentioned|map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group & Lags Supersuite.||||||
23117|Wakara Volcanic Subgroup|23616|5|Briefly described|Table 3 p46||Permian|Age: 278+/-3 Ma (Rb-Sr). Occurs mainly within the Wakera Caldera, the youngest within the Featherbed cauldron. Of Featherbed Volcanic Group, Hodgkinson Province. Thickness ~1500-2000? m.||||||
23117|Wakara Volcanic Subgroup|23713|5|Briefly described|p17||Early Permian|Of Featherbed Volcanic Group.||||||
23117|Wakara Volcanic Subgroup|24485|5|Briefly described|p45|Early Permian|Late Carboniferous|Parent: Featherbed Volcanic Group||||||
23117|Wakara Volcanic Subgroup|24486|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Featherbed Volcanics Group.  Geological Province: Kennedy province.||||||
23117|Wakara Volcanic Subgroup|43083|5|Briefly described|p84|||Of Featherbed Volcanic Group. Contains the rackarock Rhyolite.||||||17-JUN-09
23117|Wakara Volcanic Subgroup|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group.||||||15-JUN-06
23117|Wakara Volcanic Subgroup|43254|5|Briefly described|map legend||Early Permian|of Featherbed Volcanic Group||||||
23117|Wakara Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p10.||Early Permian|||||||
23117|Wakara Volcanic Subgroup|43285|5|Briefly described|Map Legend||Permian|||||||
23117|Wakara Volcanic Subgroup|43625|6|Mentioned|p36|Early Permian||||||||
23117|Wakara Volcanic Subgroup|43626|4|Described|p68||Early Permian|||||||
23117|Wakara Volcanic Subgroup|44246|5|Briefly described|Map Legend||Early Permian|||||||
23117|Wakara Volcanic Subgroup|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||
23117|Wakara Volcanic Subgroup|60425|3|Fully described|p44 Tb. 3|Early Permian|Early Permian|Of Featherbed Volcanic Gp. Contains Rackarock, Ticklehim, Gavin, Stuarts+Wollenden Rhyolites.Gavin Rh.locally over Djungan Volcanic Subgp; overlies Arringunna Rhyolite paraconform'ly;unconform. below Nychum Volcs; intruded by Bustlem+Yokas Microgranites||||||07-FEB-11
23117|Wakara Volcanic Subgroup|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Featherbed Volcanic Group.|Includes Wollenden Rhyolite.|||
23117|Wakara Volcanic Subgroup|68576|6|Mentioned|Q_11: p11-12|||Part of the Featherbed Cauldron Complex.||||||
23117|Wakara Volcanic Subgroup|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.|||A-type.|
27922|Wakeful Metabasalt Member|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Mitakoodi Quartzite (Malbon Group). Metabasalt, sandstone.||||||
27922|Wakeful Metabasalt Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27922|Wakeful Metabasalt Member|30530|2|Defined|p516|Precambrian|Precambrian|||||||
27922|Wakeful Metabasalt Member|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27922|Wakeful Metabasalt Member|39496|5|Briefly described|p5|||||||||
27922|Wakeful Metabasalt Member|39622|6|Mentioned|p19|||See also Fig.2||||||
27922|Wakeful Metabasalt Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27922|Wakeful Metabasalt Member|41791|6|Mentioned|p248|||||||||
27922|Wakeful Metabasalt Member|45166|5|Briefly described|p20|||||||||
27922|Wakeful Metabasalt Member|50100|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Mitakoodi Quartzite.  Includes basaltic lava rock.||||||15-MAR-07
27922|Wakeful Metabasalt Member|50332|5|Briefly described|p18|Proterozoic|Proterozoic|Of the Mitakoodi Quartzite. Volcanic basaltic lavas.||||||07-FEB-11
27922|Wakeful Metabasalt Member|61925|5|Briefly described|p60, p62|Paleoproterozoic|Paleoproterozoic|Of Mitakoodi Quartzite. Sequence of interbedded metapelite and quartzite and several lenses of basalt, overlying the basal conglomerate of the Mitakoodi Quartzite. See also Wakeful Basalt. Max.thickness:1400m. Geol.Prov:Leichardt Superbasin, Mt Isa Inlier||||||07-NOV-08
27922|Wakeful Metabasalt Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin||Malbon Group|||Metabasalt, minor siltstone|
27922|Wakeful Metabasalt Member|69591|6|Mentioned|p35 Fig.2.17|||Mitakoodi Domain, Mount Isa Province.||Mitakoodi Quartzite.||||
27922|Wakeful Metabasalt Member|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mitakoodi Quartzite.|||Metabasalt and minor siltstone.|
27922|Wakeful Metabasalt Member|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mitakoodi Quartzite.|||Metabasalt and minor siltstone.|
27922|Wakeful Metabasalt Member|71799|6|Mentioned|p154|||||Mitakoodi Quartzite||||
27922|Wakeful Metabasalt Member|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Mitakoodi Quartzite|||Metabasalt and minor siltstone.|
27922|Wakeful Metabasalt Member|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Mitakoodi Quartzite|||Metabasalt and minor siltstone.|
30189|Wakooka Granite|23423|5|Briefly described|p312 Table 7.4||Early Permian|S-type granite. Wakooka Supersuite.||||||
30189|Wakooka Granite|23512|5|Briefly described|Map Legend||Early Permian|||||||
30189|Wakooka Granite|43111|2|Defined|p41|Early Permian||Of Cape Melville Supersuite||||||
30189|Wakooka Granite|60425|5|Briefly described|p54 Tb. 4, p89|Early Permian|Early Permian|Of Wakooka Supersuite; formerly mapped as Altanmoui Granite. Intruded Hodgkinson Fm. S-type. Med.-gr., moderately porphyritic (muscovite-)biotite granite, with thin pegmatitic zones and rare miarolitic cavities. Further lithological details included.||||||07-FEB-11
30189|Wakooka Granite|69593|5|Briefly described|p479|Permian|Permian|Crops out over ~1 km2, south of Cape Melville in northern Hodgkinson Province.|||||Moderately porphyritic, (muscovite-) biotite granite, minor altered cordierite-tourmaline-biotite-muscovite granite.|
36715|Wakooka Supersuite|23423|4|Described|p312 Table 7.4||Early Permian|S-type granite. Intrudes Hodgkinson Formation. Also see p251. Unit was formerly part of  Altanmoui Granite.||||||
36715|Wakooka Supersuite|60425|3|Fully described|p54 Tb. 4, p89|Early Permian|Early Permian|Contains Wakooka Granite. Intrudes Hodgkinson Formation. S-type. Medium-grained, moderately porphyritic (muscovite-)biotite granite, with thin pegmatitic zones and rare miarolitic cavities.||||||07-FEB-11
77844|Walily Creek Quartz Monzodiorite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province.|||||Pinkish grey, medium-grained, slightly porphyritic biotite-hornblende granodiorite; moderately altered.|
77844|Walily Creek Quartz Monzodiorite|68679|5|Briefly described|p431, p433|Late Triassic|Late Triassic|A small unit. Assigned to this age because of similarity to the Colosseum Quartz Monzodiorite.|||||Pinkish-grey, medium-grained, slightly porphyritic  biotite-hornblende quartz monzodiorite; moderately altered.|
36310|Walkunder Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite.||||||
36310|Walkunder Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Grey, fine- to medium-grained, mainly even-grained hornblende?-biotite granite.|
26330|Wallabadah Siltstone|9528|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group. Laminated siltstone with a few thin beds of massive siltstone.||||||
26330|Wallabadah Siltstone|23291|4|Described|p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Croydon Volcanic Group. Thickness: up to 30m. Geological Province: Georgetown Region.||||||15-APR-15
26330|Wallabadah Siltstone|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26330|Wallabadah Siltstone|40659|2|Defined|p253|Mesoproterozoic|Mesoproterozoic|||||||
26330|Wallabadah Siltstone|40954|6|Mentioned|p132|||||||||
26330|Wallabadah Siltstone|41975|6|Mentioned|Fig.3 P433|||||||||
26330|Wallabadah Siltstone|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
26330|Wallabadah Siltstone|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
26330|Wallabadah Siltstone|68343|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.|||White, red-brown or purple laminated siltstone; a few thin beds of massive siltstone containing sparse sandstone cobbles; grey, very fine siltstone; minor silicified sandstone.|
26330|Wallabadah Siltstone|68345|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Is overlain conformably by B-Creek Rhyolite.|White, red-brown or purple laminated siltstone; a few thin beds of massive siltstone containing sparse sandstone cobbles; grey, very fine siltstone; minor silicified sandstone.|
26330|Wallabadah Siltstone|69591|5|Briefly described|p74 Tb.2.5, p75|||Croydon Province, Georgetown Inlier. Up to 30m ? thick. May be fluviatile deposits; very restricted distribution.||Croydon Volcanic Group.|||Laminated siltstone.|
26196|Wallabella Coal Member|24069|5|Briefly described|p283 Fig. 3|Permian|Permian|Of Tinowon Formation. Geological Province: Surat Basin.||||||
26196|Wallabella Coal Member|24077|5|Briefly described|p411 Tb. 3|Late Permian|Permian|Of the Tinowon Formation.  Black coal, carbonaceous shale and siltstone (paludal).  Max. thickness: 31m.  Geological Province: Bowen Basin.||||||
26196|Wallabella Coal Member|32578|2|Defined|p353|Late Permian|Early Permian|Early? - Late Permian||||||
26196|Wallabella Coal Member|36739|6|Mentioned|p22|||||||||
26196|Wallabella Coal Member|45110|6|Mentioned|Table 16|||||||||
26196|Wallabella Coal Member|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Of the Tinowon Formation. Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
26196|Wallabella Coal Member|63713|5|Briefly described|p1507 Fig.2, p1528|Wordian|Wordian|Roma Shelf, Bowen Basin. Appears [ambiguously] as Wallabella CM. Well-log correlation.||Unit in Tinowon Formation.||||
26196|Wallabella Coal Member|64856|4|Described|p64-65|Late Permian|Late Permian|Coal, with interbedded shale, siltstone, tuff and minor sandstone. Within the Late Permian Tinowon Formation.| | ||||29-NOV-17
26196|Wallabella Coal Member|64857|5|Briefly described|p119|Late Permian|Late Permian|Member of the Tinowon Formation, Roma Shelf, Bowen Basin.||||||
26196|Wallabella Coal Member|64858|5|Briefly described|p181|Late Permian|Late Permian|Member of the Tinowon Formation.||||||30-NOV-09
26196|Wallabella Coal Member|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Tinowon Formation or Black Alley Shale/Winnathoola CM. Underlain by Muggleton Formation.||
26196|Wallabella Coal Member|68679|5|Briefly described|p382|Permian|Permian|Similar age to the Platypus Tuff bed.||Tinowon Formation.||||
26196|Wallabella Coal Member|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Bowen Basin.|||Includes Tinowon Formation.|||
26196|Wallabella Coal Member|70878|5|Briefly described|p720 Fig.15|Permian|Permian|Bowen Basin. Appears [for reasons of space?] as Wallabella Member.||Tinowon Formation.||||
26196|Wallabella Coal Member|73304|5|Briefly described|p65, p67, p71-72|||Dating from near base of re-worked tuff within Wallabella Coal Member in Myall Creek 3 drill core. Previous SHRIMP age 257.0+/-1.5 Ma. Abbreviated to Wallabella Coal in comment on p65.|256.50+/-0.30 Ma CA-IDTIMS|Tinowon Formation||||
26196|Wallabella Coal Member|73625|6|Mentioned|p5 Fig.3|Permian|Permian|Roma Shelf, Western Bowen Basin.||||Is interbedded with Tinowon Formation.||
36340|Wallaman Falls Volcanics|23423|4|Described|p308 Table 7.3|Early Permian|Late Carboniferous|Extensively intruded by Late Carboniferous-Early Permian granites. Also see p237. Kennedy Igneous Province. Maximum thickness: 450 m.||||||
36340|Wallaman Falls Volcanics|23497|6|Mentioned|p32||Permian|||||||
36340|Wallaman Falls Volcanics|23617|3|Fully described|p15|||- Volcanic rocks in INGHAM, which are not contiguous with Glen Gordon Volcanics in ATHERTON are assigned to this unit.  - No type area has been defined. Also see Table 1 p12 + Table 3 p52. Kennedy Province.||||||
36340|Wallaman Falls Volcanics|23618|5|Briefly described|map legend|Early Permian|Late Carboniferous|||||||
36340|Wallaman Falls Volcanics|60425|4|Described|p53, p50 Tb. 3, p59 Tb. 4, p101-102|Early Permian|Late Carboniferous|Max.exposed thickness: 450m. Rhyolitic to rhyodacitic ignimbrite; + bedded silicic tuffs of Palm Islands. Rocks of 2 ages: I-type ignimbrite age: 326+/-6Ma and A-type rhyolite age: 279+/-5Ma (both SHRIMP). Intruded by rocks of Ingham Batholith.||||||07-FEB-11
36340|Wallaman Falls Volcanics|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit, as well as Elimeek Volcanics; Janet Ranges, Koolmoon, Silent Creek and Torres Strait Volcanic Groups; parts of Featherbed and Newcastle Range Volcanic Groups; and unnamed volcanic units, are all mapped under the symbol, CPvk.||||||
36340|Wallaman Falls Volcanics|69030|5|Briefly described|p6|Permian|Carboniferous|Kennedy Province.|326 +/- 6 Ma.|||||
36340|Wallaman Falls Volcanics|69593|4|Described|p495-496, p512|Permian|Late Carboniferous|Extensive outcrops in Ingham region, including volcanic units on Hinchinbrook and Palm Islands. Sm-Nd isotope data tabulated. Age poorly constrained: these SHRIMP U-Pb zircon ages for an I-type and A-type respectively, are by Branch (1966 [?]) and Rienks et al. (2000).|326 +/- 6 Ma and 279 +/- 5 Ma.|||Correlated with Glen Gordon Volcanics.|Mainly crystal-rich, biotite-bearing rhyolitic ignimbrite; subordinate crystal-poor rhyolitic ignimbrite, dacitic ignimbrite, rhyolite-dacite lava, volcanolithic sediments. Both I- and (younger) A-types.|
36340|Wallaman Falls Volcanics|70207|6|Mentioned|p82|||Ingham hinterland.|||||A-type.|
36340|Wallaman Falls Volcanics|73450|6|Mentioned|p103|Permian|Carboniferous|||||||
30379|Wallaroo Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V114. I-Type.||||||
30379|Wallaroo Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Designated as an informal name in legend.  Pale buff, white or pale grey rhyolitic ignimbrite.||||||15-JUN-06
30379|Wallaroo Rhyolite|43259|5|Briefly described|Appendix 1,p12||Late Carboniferous|Accidental formalization of Wallaroo rhyolite?||||||
77678|Wallaville Basalt|68332|5|Briefly described|Map legend.|Late Triassic|Late Triassic|Triassic Igneous Province. Age from Robertson (1992) PhD.|187.5 +/- 15.8 Ma fission track method.||||Olivine to quartz-normative tholeiitic basalt and minor bedded tuff.|15-MAR-13
77678|Wallaville Basalt|68421|5|Briefly described|Map Legend|Aalenian|Rhaetian|Triassic Igneous Province. Age determined from a site on the Bundaberg sheet area.|187.5 +/- 15.8 Ma fission track.||||Olivine to quartz-normative tholeiitic basalt and minor bedded tuff.|07-SEP-18
77886|Wallis Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Shale, siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|68146|5|Briefly described|p21|||||Wild Cow Subgroup.||Overlies Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77886|Wallis Formation|68575|5|Briefly described|p19|||South Nicholson Basin.||Wild Cow Subgroup.||Overlies Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77886|Wallis Formation|69591|5|Briefly described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Storm-dominated shelf deposits.||Wild Cow Subgroup.||Overlies Burangoo Sandstone. Is overlain unconformably by Shultz Sandstone Member (Constance Sandstone).|Shale, siltstone, thinly interbedded sandstone.|
77886|Wallis Formation|71369|4|Described|p1, p6-8, p12-14, p18-20, p24,p35,p48-49|Mesoproterozoic|Mesoproterozoic|See also p22. South Nicholson Basin. Previously the Wallis Siltstone Member (Roberts et al., 1963) of Constance Sandstone. Recognition of an overlying regional unconformity sees it raised to Formation status in this study (Sweet, 2017). Usually c.100m, up to 150m, thick. Marine shelf deposits.||Wild Cow Subgroup.||Overlies Burangoo Sandstone. Is overlain unconformably by Schultz Sandstone Member (Constance Sandstone).|Fine-grained sandstone and mudstone; laminated and thin-bedded shale and siltstone, and minor sandstone. Local ironstone beds.|20-FEB-18
77886|Wallis Formation|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Cosntance Sandstone or Schultz Sandstone Member. Underlain by Burangoo Sandstone.|Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Constance Sandstone or Schultz Sandstone Member. Underlain by Burangoo Sandstone.|Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|26-NOV-19
77886|Wallis Formation|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|||?Wild Cow Subgroup, South Nicholson Group||Overlies Burangoo Sandstone and partially and unconformably underlies Constance Sandstone.||
77886|Wallis Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Burangoo Sandstone and unconformably underlies Constance Sandstone.|Includes siltstone.|
77886|Wallis Formation|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Bunangoo Sandstone and unconformably underlies Constance Sandstone.|Includes siltstone.|
77886|Wallis Formation|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Distinct from Wallis Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77886|Wallis Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Burangoo Sandstone. Unconformably overlain by Constance Sandstone.||
77886|Wallis Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Burangoo Sandstone. Unconformably overlain by Schultz Sandstone Member (Constance Sandstone, Wild Cow Subgroup).||
35075|Wallumbilla Formation, lower|23053|6|Mentioned|p28|||||||||
35075|Wallumbilla Formation, lower|67784|6|Mentioned|p28 table 1|||||||||
27924|Wallys Dolerite|9531|5|Briefly described|Map Legend|Permian|Carboniferous|Augite dolerite with minor biotite and trace amphibole.||||||02-JUL-04
27924|Wallys Dolerite|23291|4|Described|p98 Tb. 3.11|Early Permian|Early Permian|Of the Western Georgetown Region. Age: ca.280Ma. Geological Province: Georgetown Region.||||||08-JUL-15
27924|Wallys Dolerite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 1.||||||
27924|Wallys Dolerite|40218|6|Mentioned|Map legend|Permian|Permian|||||||
27924|Wallys Dolerite|40659|6|Mentioned|p250|||||||||
27924|Wallys Dolerite|40860|4|Described|p112|Early Mesozoic|Late Paleozoic|Intrudes mid to late Proterozoic Inorunie Group.||||||07-NOV-08
27924|Wallys Dolerite|40954|6|Mentioned|p133|||||||||
27924|Wallys Dolerite|43259|4|Described|Appendix 1,p15.||Permian|||||||
27924|Wallys Dolerite|68355|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Pigeonite-augite dolerite with minor biotite and amphibole.|
27924|Wallys Dolerite|68356|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province.|||||Pigeonite-augite dolerite with minor biotite and amphibole.|
36182|Walshs Pyramid Granite|23497|5|Briefly described|Table 1||Early Permian|of Kennedy Province. Intrudes Hodgkinson Formation rocks.||||||
36182|Walshs Pyramid Granite|23507|5|Briefly described|Map Legend||Early Permian|||||||
36182|Walshs Pyramid Granite|60425|4|Described|p56 Tb. 4, p84, p274-5 Appdx. 1|Early Permian|Early Permian|Of the Bellenden Ker Supersuite. Age: 280+/-4ma (SHRIMP). S-type. One of several units of this supersuite to intrude Hodgkinson Fm. Fractionated granite - detailed lithology incuded (p275).||||||05-NOV-20
36182|Walshs Pyramid Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Part of the Bellenden Ker Batholith. Forms prominent outcrops between Cairns and Innisfail.|||||Porphyritic to even-grained (locally) (tourmaline) muscovite-biotite granite; commonly strongly foliated and partly recrystallised.|
79458|Wambo Sandstone|70628|6|Mentioned|p952 including Fig.4|Callovian|Bathonian|Said to be informally named. Also called Juandah Sandstone [the authors wrongly cite Ryan et al. 2012, who in fact mentioned the CSG industry names Juandah Sand aka Wambo Sand].||||Separates Upper and Lower Juandah Coal Measures.|Coarse-grained sandstone.
|30-JUN-16
79458|Wambo Sandstone|70725|5|Briefly described|p13|Late Jurassic|Late Jurassic|Surat Basin.||Walloon Coal Measures.||Overlies Lower Juandah Coal Measures. Is overlain by Upper Juandah Coal Measures.||
79458|Wambo Sandstone|71282|6|Mentioned|p456, p457 Fig.1, p467|||Attributed to Ryan et al. (2012). Said to be also referred to as the Juandah Sandstone (Silwa and Esterle, 2008).||||||
78847|Wambo seam package|65096|6|Mentioned|p372, 376|Middle Jurassic|Middle Jurassic|[informal 'sequence stratigraphy' unit] 'seam package' of Juandah Coal Measures. See also fig.2, p370. Difficult to distinguish from Kogan and MacAlister seam packages on basis of wireline logs.||Said to be of the Juandah Coal Measures sequence.||Between overlying MacAlister and underlying Iona seam packages.||
24074|Wando Vale Subgroup|23032|5|Briefly described|p25 fig6||Devonian|||||||
24074|Wando Vale Subgroup|23423|5|Briefly described|Plate 8.4d|||||||||
24074|Wando Vale Subgroup|23424|5|Briefly described|Table 8.1|Middle Devonian|Early Devonian|Of Broken River Group, Graveyard Creek Subprovince.||||||
24074|Wando Vale Subgroup|23431|5|Briefly described|p541|||||||||
24074|Wando Vale Subgroup|41260|4|Described|p118|||See also Table 1. Mention P163||||||
24074|Wando Vale Subgroup|41679|2|Defined|p255|Givetian|Emsian|||||||
24074|Wando Vale Subgroup|41719|6|Mentioned|Fig.2|||||||||
24074|Wando Vale Subgroup|41739|6|Mentioned|Fig.2|||||||||
24074|Wando Vale Subgroup|41740|6|Mentioned|p222|||||||||
24074|Wando Vale Subgroup|42031|5|Briefly described|Fig.5 P762|||||||||
24074|Wando Vale Subgroup|42054|6|Mentioned|p273|||||||||
24074|Wando Vale Subgroup|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
24074|Wando Vale Subgroup|42709|6|Mentioned|map legend|||||||||
24074|Wando Vale Subgroup|42933|4|Described|p79|||Of Broken River Group.||||||18-MAR-08
24074|Wando Vale Subgroup|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Broken River Group.||||||
24074|Wando Vale Subgroup|43603|5|Briefly described|p9|Carboniferous|Late Devonian|||||||
24074|Wando Vale Subgroup|63154|5|Briefly described|p281 Fig. 3|Early Devonian|Early Devonian|Of the Broken River Group. Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
24074|Wando Vale Subgroup|64707|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Broken River Group. Mudstone (commonly calcareous and fossiliferous), lithofeldspathic, subfeldspathic and quartzose sandstone, polymictic conglomerate and limestone.||||||
24074|Wando Vale Subgroup|68336|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Broken River Group.|Includes Tank Creek and Storm Hill Sandstones; Lomandra, Chinaman Creek, Dip Creek, Lockup Well, Jessey Springs and Dosey Limestones; Bracteata and Papilio Mudstones, and Burges Formation.||Mudstone (commonly calcareous and fossiliferous), lithofeldspathic, subfeldspathic and quartzose sandstone, polymictic conglomerate and limestone.|
24074|Wando Vale Subgroup|68338|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Broken River Group.|||Mudstone (commonly calcareous and fossiliferous), lithofeldspathic, subfeldspathic and quartzose sandstone, polymictic conglomerate and limestone.|
24074|Wando Vale Subgroup|68341|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Broken River Group.|Includes Tank Creek and Storm Hill Sandstones; Lomandra, Chinaman Creek, Dip Creek, Lockup Well, Jessey Springs and Dosey Limestones; Bracteata and Papilio Mudstones, and Burges Formation.||Mudstone (commonly calcareous and fossiliferous), lithofeldspathic, subfeldspathic and quartzose sandstone, polymictic conglomerate and limestone.|
24074|Wando Vale Subgroup|68478|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Broken River Group.|Includes Papilio Mudstone, Dosey Limestone, Storm Hill Sandstone, Burges Formation, Lomandra Limestone, and Bracteata Mudstone.|||
24074|Wando Vale Subgroup|68479|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Broken River Group.|Includes Papilio Mudstone, Dosey Limestone, Storm Hill Sandstone, Burges Formation, Lomandra Limestone, and Bracteata Mudstone.|||
24074|Wando Vale Subgroup|69030|5|Briefly described|p6|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province).||Broken River Group.||||
29113|Wandsworth Volcanic Group|721|5|Briefly described|Map legend|Late Permian|Late Permian|Undifferentiated rock of this group is represented on this sheet - rhyolitic to rhyodacitic ashflow tuffs and rare lavas, rare trachyte, and andesite.||||||
29113|Wandsworth Volcanic Group|22490|4|Described|4|Late Permian|Late Permian|Geol province New England Fold Belt.||||||24-SEP-08
29113|Wandsworth Volcanic Group|22580|6|Mentioned|p97,p99||Late Permian|||||||
29113|Wandsworth Volcanic Group|22857|5|Briefly described|p262, p536 App.1 Tb.A1.9|Early Triassic|Late Permian|Contains the Coombadhja Volcanic Complex. Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|22864|5|Briefly described|p262,264|||||||||
29113|Wandsworth Volcanic Group|23050|4|Described|p14 Table 1|Late Permian|Late Permian|Age: unconformably overlies Sandon beds and is intruded by Early Triassic granites.||||||
29113|Wandsworth Volcanic Group|23051|5|Briefly described|Map Legend|Late Permian|Early Permian|||||||
29113|Wandsworth Volcanic Group|23544|6|Mentioned|p372|||||||||
29113|Wandsworth Volcanic Group|23720|5|Briefly described|Map Legend|||Includes the Annalee Pyroclastics and other volcanics, and the Dummy Creek Conglomerate.||||||15-DEC-04
29113|Wandsworth Volcanic Group|23763|5|Briefly described|p543 Fig. 1|Permian|Permian|Includes the Gilgurry Mudstone, Drake Volcanics, Dundee Rhyodacite and Coombadja Volcanic Complex.  Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|23790|5|Briefly described|p10 Fig. 2|Late Permian|Late Permian|Geological Province: Central Block.||||||28-OCT-08
29113|Wandsworth Volcanic Group|23811|5|Briefly described|Map Legend|Permian|Early Permian|Includes the Tent Hill, Emmaville, Wallangarra and Drake Volcanics, Gibraltar Ignimbrite and the Coombadjha Volcanic Complex, as well as undifferentiated Wandsworth Volcanic group and seven informally (geographic) named masses of the Dundee Rhyodacite.||||||31-MAY-07
29113|Wandsworth Volcanic Group|23812|4|Described|p25, p26 Tb.3|Early Triassic|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|23859|5|Briefly described|p930|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|24366|5|Briefly described|p9, 17 Fig. 3|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|24480|5|Briefly described|p7|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|42378|2|Defined|p2-30|Early Triassic|Late Permian|Encompasses 8 named units and undifferentiated Permian volcanics.||||||
29113|Wandsworth Volcanic Group|42559|6|Mentioned|p10|||||||||
29113|Wandsworth Volcanic Group|42719|5|Briefly described|p7|||||||||
29113|Wandsworth Volcanic Group|42729|5|Briefly described|p12|||||||||
29113|Wandsworth Volcanic Group|42748|6|Mentioned|Fig.3 P9|Permian||||||||
29113|Wandsworth Volcanic Group|43017|5|Briefly described|Fig.2,p374|||||||||
29113|Wandsworth Volcanic Group|43091|5|Briefly described|Map legend|||||||||
29113|Wandsworth Volcanic Group|44093|5|Briefly described|p233 App. 1|Late Permian|Early Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|44450|3|Fully described|p25|Permian|Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|60079|5|Briefly described|Map Legend|Late Permian|Permian|Includes: Dundee Rhyodacite.||||||
29113|Wandsworth Volcanic Group|60422|5|Briefly described|p386, Fig. 1|Upper Permian|Upper Permian|||||||
29113|Wandsworth Volcanic Group|61772|6|Mentioned|p128, p133, p131||Late Permian|Thick, bedded felsic volcanic rocks. In southern New England Orogen.||||||27-MAY-08
29113|Wandsworth Volcanic Group|61773|6|Mentioned|p138|||||||||
29113|Wandsworth Volcanic Group|61793|6|Mentioned|p341|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||07-FEB-11
29113|Wandsworth Volcanic Group|61796|5|Briefly described|p385, p386 Fig. 1|Late Permian|Late Permian|Geological Province: New England Fold Belt.||||||
29113|Wandsworth Volcanic Group|61804|5|Briefly described|p419|Permian|Permian|Felsic rocks. Geological Province: New England Fold Belt.||||||28-OCT-08
29113|Wandsworth Volcanic Group|62534|4|Described|p6, p7|Early Triassic|Late Permian|Of Barnes et al (1991). Comprises Emmaville and Tent Hill Volcanics and Dundee Rhyodacite - each characterised by distinctive magnetic and/or radiometric features.||||||07-FEB-11
29113|Wandsworth Volcanic Group|62757|5|Briefly described|p3 Fig. 1|Late Permian|Late permian|Felsic volcanic units.||||||07-FEB-11
29113|Wandsworth Volcanic Group|63347|5|Briefly described|p2|Late Permian|Late Permian|Geological Province: New England Orogen.||||||
29113|Wandsworth Volcanic Group|63748|6|Mentioned|p16, p50|Late Permian|Middle Permian|Of Barnes et al (1991) in New South Wales - see Wandsworth Group, although the two terms are used interchangeably in the text.||||||07-FEB-11
29113|Wandsworth Volcanic Group|65398|5|Briefly described|p4 Fig.2, p8-9, Fig 2-3|Late Permian|Late Permian|Thermally metamorphosed ignimbritic, rhyolitic and rhyodacitic volcaniclastic rocks: ashflow tuffs, local sandstone and conglomerate. Unconformably overlies Cara Formation; is intruded by Attunga Creek Monzogranite.||||||
29113|Wandsworth Volcanic Group|65668|6|Mentioned|p2, p32|Late Permian|Late Permian|Includes the Wallangarra and Emmaville Volcanics, considered to be closely related (Barnes et al., 1991 and Purdy, 2003). Age c.254 Ma. Dominantly calc-alkaline, terrestrial ignimbrites to shallow marine volcanics, deposited over large areas of the central New England region.||||||
29113|Wandsworth Volcanic Group|66720|5|Briefly described|Map legend|Early Triassic|Late Permian|The volcanic and sedimentary rocks are mapped separately, but with no Member status or names.|||||Rhyolitic to rhyodacitic volcaniclastic rocks; undifferentiated interbedded pebble conglomerate and feldspathic and lithic sandstone.|
29113|Wandsworth Volcanic Group|68005|5|Briefly described|p18, pp42-46, p69 Fig.3-S, pp151-153.|Late Permian|Late Permian|Central Block, New England Fold Belt. A coherent group of terrestrial and shallow marine felsic volcanics.|||Includes Emmaville and Wallangarra Volcanics, Gibraltar Ignimbrite.||Undifferentiated felsic volcanics, minor sediments and granites. Dominantly ignimbritic rhyolites and rhyodacites (dark crystal-lithic tuffs); rhyodacitic lavas, minor dacite, andesite, trachyte; interbedded fine-grained tuff and volcaniclastics.|
29113|Wandsworth Volcanic Group|68006|5|Briefly described|p20 Fig.3-A, p26, p115.|||Central Block, New England Fold Belt. Of Barnes et al. (1991).|||Includes Emmaville Volcanics and Glenmore Formation.||Thick sequences of predominantly rhyolitic to rhyodacitic, and minor andesitic, tuffs and ignimbrites.|
29113|Wandsworth Volcanic Group|68111|5|Briefly described|p968 Tb.1, p973||||||Includes Drake Volcanics, Dundee Rhyodacite, Emmaville Volcanics, and Wallangarra Volcanics.|||
29113|Wandsworth Volcanic Group|68553|6|Mentioned|Map legend|Permian|Permian|||||||
29113|Wandsworth Volcanic Group|68679|5|Briefly described|p451, p453|Permian|Permian|Barnes et al. (1991). Wandsworth Province. Largely undeformed.|||Wallangarra Volcanics, Dundee Rhyodacite.|Correlated with the Texas beds.||
29113|Wandsworth Volcanic Group|68822|6|Mentioned|p339|Late Permian|Late Permian|||||||
29113|Wandsworth Volcanic Group|69188|5|Briefly described|p1, p60, p64|||Same age as Culaden Granodiorite.|||Emmaville Volcanics.|Is overlain by Dundee Rhyodacite.||
29113|Wandsworth Volcanic Group|69323|5|Briefly described|p1,3,13-33,41,70-71, 76|Lopingian|Lopingian|Geological province: New England Orogen. Commonly abbreviated WVG in text. Traditionally regarded as having the Drake Volcanics at its base, but not anymore based on the age of the Drake Volcanics (264.4+\-2.5 Ma; Cross and Blevin 2010), and that it has a distinct chemical composition to the Wandsworth Volcanic Group.|||Includes Emmaville Volcanics, Emmaville Volcanics, 'Uralla volcanics', 'Attunga Creek volcanics', 'Kurrajong Park volcanics'.|||03-DEC-19
29113|Wandsworth Volcanic Group|69639|4|Described|p2, p8-p9, p16, p21|Lopingian|Lopingian|New England Orogen. Contact metamorphosed by the Attunga Creek Monzogranite. Also intruded by Mount Jonblee Leucomonzogranite, Mole Granite, Kingsgate Leucogranite, Wards Mistake Monzogranite and the Mount Mitchell Monzogranite. See also p26, p38, p44, p50, p62, p94, p212, p218-p222.|255.8 +/- 1.5 Ma (Chisholm et al, 2014)||Includes the Dundee Rhyodacite, Attunga Creek volcanics and the Wallangara Volcanics.|Intruded by the Attunga Creek Monzogranite, Dandahra Creek Leucogranite, Bolivia Range Leucomonzogranite.||
29113|Wandsworth Volcanic Group|70217|5|Briefly described|p38, p43, p49, p75|||New England Orogen. Ages derived from Cross and Blevin, 2010, 2013 and from Chisholm et al, 2014a. |256-252 Ma||Includes the Wandsworth Volcanics.|Intrudes the Webbs Consols Leucogranite. Intruded by the Pyes Creek Leucomonzogranite.||
29113|Wandsworth Volcanic Group|70876|5|Briefly described|p2, p64, p70, p79, p81|Late Permian|Middle Permian|New England Orogen. Previously included the Drake Volcanics; in this study they are recognised as a distinct unit on the basis of geochronology. Represents extensive terrestrial and shallow marine volcanism. Previously this group has been dated either Triassic or Permian but recent modern U-Pb dating techniques have placed the group firmly in the Permian.|||Includes the Wallangarra Volcanics, Emmaville Volcanics and Dundee Rhyodacite.|||
29113|Wandsworth Volcanic Group|71628|5|Briefly described|p3-52; p7: 2, 5, 40; p8: 16, 34, 40, 44|||See also p8: 50, 56, 61, 65-66, 72, 76, 80, 86-87, 92; p10-3; p11: 10-11, 20, 23, 26; p12: 5, 18; p13-4; p14: 3, 7, 12, 28; p15: 5, 9, 12, 22, 25, 29, 31, 106; p17: 4-5; p19: 43, 72, 77, 110, 141, 144-145, 159-160. A pendant of these rocks occurs in the Attunga Creek Monzogranite; probably comagmatic and representing cauldron collapse. See also Wandsworth Volcanics (p8: 13, 25, 28; p10-9; p11-11; p15-67; p19: 55, 77, 142). CONSTITUENTS (continued): Nioka Porphyritic Dacite; Arranmor, Pi Pi Ignimbrites; Georges Mountain Volcanics; Coombadjha Volcanic Complex. RELATED UNITS (continued): Is intruded by Walcha Road, Mount Duval, Cottesbrook, Llangothlin, Wards Mistake Monzogranites; Khatoun and Wilhelmshohe Tonalites; Manuka Farm and Terrible Vale Porphyritic Microgranodiorites; Uralla Granodiorite; Glen Garry Microleucosyenogranite; Mount Jonblee, Billyrimba, Bolivia Range, Clive and Sandy Flat Leucomonzogranites; Gilgai and Mole Leucogranites; Deepwater Syenogranite and Kentucky Quartz Diorite. May be intruded by The Basin and Tingha Monzogranites (no contacts observed). Abuts Mount Mitchell and Strathaven Monzogranites.|||Annalee Pyroclastics; Dummy Creek Conglomerate; Dundee Rhyodacite; Abington, Baldersleigh, Emmaville, Pheasant Creek, Tent Hill, Wallangarra Volcanics. See COMMENTS for more.|Overlies Henry River and (locally) Wellingrove Monzogranites. Is faulted against Rocky River Monzogranite and Dandahra Creek Leucosyenogranite. See COMMENTS for more.|Includes felsic volcanics.|
29113|Wandsworth Volcanic Group|72528|6|Mentioned|p71.|||Field relationships indicate a close temporal correlation with Deepwater Syenogranite.|||Includes Emmaville Volcanics.|||
24557|Wangetti Granite|12575|6|Mentioned|p784 Table 1.|||Apatite fission track analyses are detailed.|285-273 Ma.|||||
24557|Wangetti Granite|22497|5|Briefly described|p108|||||||||
24557|Wangetti Granite|23423|5|Briefly described|p312 Table 7.4||Early Permian|S-type. Also see p246.  Of Wangetti Supersuite.||||||
24557|Wangetti Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 393. S-Type.||||||
24557|Wangetti Granite|42625|5|Briefly described|Map legend|Triassic|Late Permian|Reserved.||||||
24557|Wangetti Granite|42810|2|Defined|Table 1 P16|Early Triassic|Late Permian|see also p24.||||||01-JUN-09
24557|Wangetti Granite|43259|4|Described|Appendix 1,p44.||Early Permian|Age is 259-285 Ma.||||||
24557|Wangetti Granite|60425|4|Described|p56 Tb. 4, p83|Early Permian|Early Permian|Of the Wangetti Supersuite. Age between 273 Ma and 285Ma. Intrudes Hodgkinson Formation. S-type, medium-gr., even-gr. to highly porphyritic, tourmaline-muscovite granite and (tourmaline-) muscovite-biotite granite; miarolotic cavities common. S-type.||||||14-JUN-13
24557|Wangetti Granite|68576|5|Briefly described|Q_11: p3|Permian|Permian|Wangetti Beach. Geochemically distinct and unfoliated; occurs amongst Mount Formartine Granite plutons. Early Permian. K-Ar biotite ages of 255-235 Ma record post-deformation (D4) uplift and cooling.|285-273 Ma (whole-rock Rb-Sr age).|||||
24557|Wangetti Granite|69593|5|Briefly described|p479, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~3 km2 N of Cairns as small, roughly concentric plutons or zones. Age poorly constrained. Sm-Nd isotope data tabulated.|280 Ma.|Wangetti Suite.|||S-type. Even-grained to highly porphyritic, tourmaline-muscovite and (tourmaline-) muscovite-biotite granite; miarolitic cavities common.|
24557|Wangetti Granite|72297|5|Briefly described|p718|||Hartley's Creek, 37km NW of Cairns. Tantalite and cassiterite occur in quartz pegmatite and quartz veins.||||||
36716|Wangetti Suite|23423|5|Briefly described|p312 Table 7.4||Early Permian|S-type. Of Wangetti Supersuite.||||||
36716|Wangetti Suite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Brodies Camp, Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto and Tinaroo Suites; and various ungrouped Permian plutonic units.||||||
36716|Wangetti Suite|69593|5|Briefly described|p478-480, p505, p506 Fig.6.26, p511|||Daintree Subprovince, Kennedy Igneous Association. Crops out over ~3 km2 N of Cairns as small, roughly concentric plutons or zones. Geochemistry briefly described.|||Wangetti Granite.||Very strongly fractionated S-type. Even-grained to highly porphyritic, tourmaline-muscovite and (tourmaline-) muscovite-biotite granite; miarolitic cavities common.|
33901|Wangetti Supersuite|22497|6|Mentioned|p106 Fig.1|Early Permian|Early Permian|||||||
33901|Wangetti Supersuite|23423|4|Described|p312 Table 7.4||Early Permian|Age: 273-285 Ma. S-type granites. Also see p246-247.||||||
33901|Wangetti Supersuite|23430|6|Mentioned|p493|||||||||
33901|Wangetti Supersuite|60425|4|Described|p56 Tb. 4|Early Permian|Early Permian|Comprises just Wangetti Granite. Age between 273ma and 285Ma. Intrudes Hodgkinson Formation. S-type, medium-gr., even-gr. to highly porphyritic, torumaline-muscovite granite and (torumaline-) muscovite-biotite granite; miarolotic cavities common.||||||07-FEB-11
33901|Wangetti Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|||||S-type granitoids.|
37052|Wappa Rhyolite|23251|5|Briefly described|Table 1, p8||Late Triassic|No isotopic dating; relationship to other units indicates a Late Triassic age. See also Wappa Rhyolite Member Table 3 p25 - names used interchangeably.||||||21-JUN-06
37052|Wappa Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
37052|Wappa Rhyolite|44928|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics Group.||||||31-MAY-06
37052|Wappa Rhyolite|68679|5|Briefly described|p436 Fig.5.97, p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.|||Thick, strongly flow-banded rhyolite lava flows with microcrystalline to subtrachytic texture.|
37052|Wappa Rhyolite|69952|6|Mentioned|p47|||||Unit in North Arm Volcanic Group.||||
37052|Wappa Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
36683|Warby Volcanic Subgroup|23291|3|Fully described|p38, 39,  p93 Tb. 3.9|Late Carboniferous|Late Carboniferous|Formerly Warby Volcanics"". Parent: Bulleringa Volcanic Subgroup. Thickness: 115m. Geological Province: Georgetown Region.||||||08-JUL-15
36683|Warby Volcanic Subgroup|23616|5|Briefly described|Table 3 p53||Late Carboniferous|Age: Late Carboniferous? Intruded by Late Carboniferous granitoids. Of Scardons Volcanic Group. Dargalong Province. Maximum thickness ~200 m.||||||
36683|Warby Volcanic Subgroup|68405|5|Briefly described|Map Legend|Permian|Late Carboniferous|Kennedy Province. Early Permian ? minimum age. Shown as two groups of unnamed units; a Late Carboniferous group, and an Early Permian? Group. See map legend for lithological description.||Of the Scardons Volcanic Group.|Informally subdivided on this map into 3 unnamed units.|Unconformably underlain by the Blackman Gap Complex. Shown as equivalent age to Bulleringa Volcanic Subgroup.|Rhyolite, rhyolitic ignimbrite, dacite lava, dacitic breccia.|
75609|Ward Creek Granite|70673|4|Described|p5-6, p10, p121-124|Late Carboniferous|Late Carboniferous|Abbreviated to Ward Creek GD on p6. Appears as Ward Creek Granodiorite on p9. Indistinguishable from ages for adjacent Milwarra Quartz Diorite and Tommy Roundback Granodiorite. Previously dated as Late Jurassic to Early Cretaceous (details given).|323.0 +/- 1.8 Ma (SHRIMP U-Pb zircon).||||White, medium-grained, slightly to moderately porphyritic biotite granodiorite, containing scattered mafic enclaves up to c.40 cm across. Moderately deformed.|24-MAR-17
75609|Ward Creek Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen. Metamorphosed at c.298 Ma and c.288 Ma.|323+/-1.8 Ma (MDA: U-Pb zircon SHRIMP)||||Granodiorite.|
40141|Warminster Formation|24615|5|Briefly described|CD|Permian|Permian|[Pw].  Sandstone, volcaniclastic breccia.||||||
40141|Warminster Formation|50212|5|Briefly described|Map Legend|Permian|Permian|||||||
40141|Warminster Formation|60557|5|Briefly described|p18 Fig. 5a|Early Permian|Early Permian|||||||
40141|Warminster Formation|61778|2|Defined|p234 Fig. 1, p239, p241, p240 Fig. 11|late Permian|Late Permian|Underlain unconformably by Chalmers Formation (Berserker Gp). Thikness: 100m. Composed of sandstone and polymitic breccia. Geol Prov: Berserker Subprovince. See p239-241 for detailed info. Shallow marine environment.||||||07-FEB-11
40141|Warminster Formation|64429|2|Defined|p15, p23|Late Permian|Late Permian|Formerly included in Berserker Series and Berserker beds. Unconformable on Berserker Gp. Dark green-grey, fine to coarse, well-sorted sst; other rock type is dark green-grey, massive, poorly sorted, matrix-supported, granule to pebble polymictic breccia||||||
40141|Warminster Formation|68008|2|Defined|p158-159, p173, p175-176, p483, p570|Permian|Permian|Originally a part of the Berserker Series (Whitehouse, 1930), renamed the Berserker beds (Kirkegaard et al., 1970), which was divided into the Berserker Group and this unit (Crouch and Parfrey, 1998). Covers only 300m2, which constitutes the type area. Named after Mount Warminster. Thickness estimated up to 100m. Appears also as Mount Warminster Formation on p159 and p173. Late Permian. Fossils are of the same age as those in Barfield, Flat Top, Ingelara and Peawaddy Formations in the Bowen Basin.||||Disconformably or unconformably overlies Berserker Group. Age-equivalent to Moah Creek beds.|Dark green-grey, fine to coarse, well sorted sandstone; dark green-grey, massive, poorly sorted, matrix supported, granule to pebble polymictic breccia. Strongly silicified and chloritised.|
40141|Warminster Formation|68679|5|Briefly described|p350|Permian|Permian|Crouch and Parfrey (1998). Covers 300 m2. Bivalve and gastropod fossils, known in several Formations (listed) in the Bowen Basin, determine the late Permian age and suggest a disconformity with the underlying unit. This is the current formal name; see also references to Mount Warminister Formation (p338) and Mount Warminster Formation (also on p350).||||Disconformably overlies the Berserker Group.|Fine- to coarse-grained sandstone; massive, poorly-sorted, matrix-supported, granule to pebble polymict breccia, with a sandy matrix and angular volcanic, siltstone and chert clasts to 30mm.|
26287|Warner Granite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Ebagoola Suite||||||
26287|Warner Granite|22781|4|Described|p34|Paleozoic|Paleozoic|Ebagoola Suite||||||07-NOV-08
26287|Warner Granite|42610|2|Defined|p11|Early Devonian|Early Devonian|Age assumed same as Barwon Granite.||||||
26287|Warner Granite|43596|4|Described|p32, p28 Tb. 3|||Pale grey to buff equigranular muscovite-biotite granite, foliated in places. Unassigned granite.||||||15-JAN-09
26287|Warner Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
24080|Warrior Diorite|23513|5|Briefly described|Map legend|Devonian||Palaoezoic Intrusive No. 450.||||||
24080|Warrior Diorite|41668|6|Mentioned|p28|||||||||
24080|Warrior Diorite|42054|6|Mentioned|p272|||||||||
24080|Warrior Diorite|43259|4|Described|Appendix 1,p48.||Cambrian|Pre-Ordivician?.||||||
38866|Warrong Teschenite|24488|5|Briefly described|Map Legend|Cretaceous|Triassic|||||||
38866|Warrong Teschenite|24615|5|Briefly described|CD|Cretaceous|Triassic|[Mgwa].  Grey medium-grained ophitic olivine-titanaugite teschenite, locally banded.||||||
38866|Warrong Teschenite|68008|3|Fully described|p213, p438-440|Mesozoic|Mesozoic|New unit: a small body on the crest of Dawes Range c.30km N of Monto, between Pine Mountain Creek and Warrong Creek (after which it is named). The type area is along the W side of the track S from Dooloo Tops homestead. Geophysics briefly described. No geochemical analysis done.||||Intrudes Dooloo Tops Volcanics (assumed).|Grey, medium-grained gabbroic rock showing poorly defined compositional banding.|
25604|Washpool Creek Formation|31586|5|Briefly described|p6|||Correlation of Visean Coral horizons||||||
25604|Washpool Creek Formation|31587|6|Mentioned|p59|||Geological map||||||
25604|Washpool Creek Formation|32388|6|Mentioned|Fig.1|||||||||
25604|Washpool Creek Formation|32866|6|Mentioned|Fig.12|||||||||
25604|Washpool Creek Formation|33774|6|Mentioned|p21|||Tourn.- Visean boundary at top of Fm.||||||
25604|Washpool Creek Formation|34085|6|Mentioned|Cor.chart|||Tourn-Visean||||||
25604|Washpool Creek Formation|36528|6|Mentioned|p172|||||||||
25604|Washpool Creek Formation|42547|4|Described|p51|||||||||
25604|Washpool Creek Formation|44360|14|Not recorded|p10,30,32||Early Carboniferous|May be equivalent to Splinter Creek Formation.||||||
25604|Washpool Creek Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
25604|Washpool Creek Formation|46803|6|Mentioned|Fig. 4|||||||||
26987|Watalgan Granite|9194|5|Briefly described|Map legend|Triassic|Triassic|Granite, granodiorite, minor quartz diorite.||||||12-JUL-04
26987|Watalgan Granite|30655|3|Fully described|p37|||||||||
26987|Watalgan Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
26987|Watalgan Granite|32137|6|Mentioned|p355|||||||||
26987|Watalgan Granite|39445|5|Briefly described|Table 12|||||||||
26987|Watalgan Granite|43995|14|Not recorded|Tb.p10||Jurassic|||||||
26987|Watalgan Granite|44752|14|Not recorded|p299,301|||intrudes Brooweena Formation. Similar age to Mount Bauple Syenite.||||||
26987|Watalgan Granite|45440|14|Not recorded|p.34|||||||||
26987|Watalgan Granite|67203|5|Briefly described|p3|Triassic|Triassic|||||||
26987|Watalgan Granite|68421|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Triassic Igneous Province. The 2 facies are mapped separately.|||||Leucocratic biotite granite, biotite granodiorite, biotite-hornblende quartz diorite, aplite; fine to medium-grained biotite leucogranite, in places with strong granophyric textures; common feldspar porphyry dykes.|
26987|Watalgan Granite|68679|5|Briefly described|p428, p433|Late Triassic|Late Triassic|Northern New England Orogen.|||||Fine- to medium-grained, leucocratic biotite granite, granophyric in places; biotite granodiorite, biotite-hornblende quartz diorite, aplite; common feldspar porphyry dykes.|
26987|Watalgan Granite|73450|6|Mentioned|p16|||||||||
28013|Watch Branch Monzogranite|23420|5|Briefly described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intruded by Morehead Granite and Wipella Granodiorite||||||
28013|Watch Branch Monzogranite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Dinah Formation, Sugarbag Creek Quartzite and Wipella Granite(?). Medium to dark grey equigranular biotite monzogranite.||||||15-JAN-09
28013|Watch Branch Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
40848|Watch Hill Granodiorite|50200|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
40848|Watch Hill Granodiorite|50202|5|Briefly described|Map legend|Late Silurian|Late Silurian|(Muscovite)-biotite granodiorite; minor pegmatite and aplite veins.||||||
40848|Watch Hill Granodiorite|68336|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith.|||||Grey, locally foliated, medium-grained, equigranular (muscovite)-biotite granodiorite; minor muscovite pegmatite and aplite veins.|
40848|Watch Hill Granodiorite|68341|5|Briefly described|Map legend.|Silurian|Silurian|Dido Batholith.|||||Grey, locally foliated, medium-grained, equigranular (muscovite)-biotite granodiorite; minor muscovite pegmatite and aplite veins.|
40848|Watch Hill Granodiorite|68344|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Dido Batholith, Thalanga Province. |||||Grey, locally foliated, medium-grained, equigranular (muscovite-)biotite granodiorite; minor muscovite pegmatite and aplite veins.|
40848|Watch Hill Granodiorite|68410|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Dido Batholith.|||||Grey, locally foliated, medium-grained equigranular (muscovite)-biotite granodiorite; minor muscovite pegmatite and aplite veins.|
40848|Watch Hill Granodiorite|69592|6|Mentioned|p283|Silurian|Silurian|||Dido Supersuite.||||
26988|Wateranga Gabbro|24382|5|Briefly described|Map legend|Triassic|Permian|||||||
26988|Wateranga Gabbro|29960|4|Described|p10|||||||||
26988|Wateranga Gabbro|30654|4|Described|p46|||Permian age. See also P47,49,55,57.||||||
26988|Wateranga Gabbro|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
26988|Wateranga Gabbro|35520|5|Briefly described|p32|||Petrography and mineralogy||||||
26988|Wateranga Gabbro|39445|5|Briefly described|Table 12|||||||||
26988|Wateranga Gabbro|40475|6|Mentioned|p7|||||||||
26988|Wateranga Gabbro|40919|6|Mentioned|Fig.2|||||||||
26988|Wateranga Gabbro|41594|6|Mentioned|p50|||||||||
26988|Wateranga Gabbro|41736|6|Mentioned|p117|||||||||
26988|Wateranga Gabbro|41778|6|Mentioned|Fig.1|||||||||
26988|Wateranga Gabbro|43008|5|Briefly described|map legend|||||||||
26988|Wateranga Gabbro|45440|2|Defined|p.54,55,81|||Tb.1. Permian?||||||
26988|Wateranga Gabbro|63821|5|Briefly described|p29|Triassic|Permian|Age: 244+/-8Ma (K-Ar hornblende). Intrudes the Good Night beds. Layered olivine gabbro.||||||07-FEB-11
26988|Wateranga Gabbro|65388|5|Briefly described|p323|Triassic|Permian|One of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton.||||||
26988|Wateranga Gabbro|68008|6|Mentioned|p435|||One of a chain of gabbro intrusions (listed) between Brisbane and Rockhampton.||||||
26988|Wateranga Gabbro|68679|5|Briefly described|p420-422|Middle Triassic|Early Triassic|Gayndah-Gladstone belt. ~22 km2. First drilled in the 1960s (Robertson, 1971). Funnel or laccolith shape. One of four similar ages given.|245 +/- 7 Ma (K-Ar: Green, 1975).|||Intrudes the Good Night beds. Is adjacent to Mingo Granite.|Layered olivine gabbro, gabbronorite, olivine gabbronorite, anorthosite, minor granite; mesocumulates to adcumulates. Layering gradational on millimetre to metre scale; three zones correspond to magma replenishment pulses.|
26988|Wateranga Gabbro|72297|6|Mentioned|p721, p726, p728|||The Wateranga prospect contains large deposits of apatite and feldspar, with minor corundum, zircon and rutile, in alluvial, eluvial and hard rock deposits.||||||
30007|Waterfall Granite|23511|5|Briefly described|Map Legend|Late Permian|Early Permian|Of Cooktown Supersuite.||||||08-OCT-08
30007|Waterfall Granite|43070|6|Mentioned|p66|||||||||
30007|Waterfall Granite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Cooktown Supersuite. Porphyritic biotite granite.||||||
30007|Waterfall Granite|60425|4|Described|p270-1 Appdx. 1d|||Of Waterfall Suite (Cooktown Supersuite). S-type. Fine-gr., highly porphyritic (altered cordierite)-musc.-tourm.-biot.granite; qtz phenocrysts locally deeply embayed; sparse enclaves (to 10cm) of 'microdiorite'+biotite-rich gneiss; extensively deformed||||||07-FEB-11
30007|Waterfall Granite|69593|5|Briefly described|p479, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|270 Ma.|Waterfall Suite.|||S-type granitoids.|
36721|Waterfall Suite|23423|5|Briefly described|Table 7.1 p240|||Of Cooktown Group.||||||
36721|Waterfall Suite|60425|4|Described|p81 Tb. 5, p270-1 Appdx. 1|Early Triassic|Late Permian|Of Cooktown Supersuite. Contains Waterfall Granite. S-type. Age: 270-247Ma (est.) (Rb-Sr).||||||07-FEB-11
36721|Waterfall Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Cooktown Supersuite.|Waterfall Granite.||S-type granitoids.|
38207|Waterloo Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Ordovician|||||||
38207|Waterloo Supersuite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
24083|Watershed North Rhyolite|23422|4|Described|p181, p205 Table 6.3|Early Carboniferous|Early Carboniferous|Intruded by Speed Creek Granite. Maximum thickness: ~415m.  Overlying Unit: Insolvency Gully Formation.||||||
24083|Watershed North Rhyolite|23430|6|Mentioned|p489|||||||||
24083|Watershed North Rhyolite|23431|5|Briefly described|p538|||||||||
24083|Watershed North Rhyolite|23509|5|Briefly described|Map Legend||Carboniferous|||||||
24083|Watershed North Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V60. I-Type.||||||
24083|Watershed North Rhyolite|23893|5|Briefly described|p18|Carboniferous|Carboniferous|Of Oweenee Supersuite.  Geological Province: Kennedy Province.||||||21-APR-08
24083|Watershed North Rhyolite|24613|6|Mentioned|p147|||Probably misspelt - see Watershed Rhyolite.||||||20-JUN-13
24083|Watershed North Rhyolite|42689|5|Briefly described|map legend|Carboniferous||||||||
24083|Watershed North Rhyolite|43095|2|Defined|p33|Early Carboniferous||||||||
24083|Watershed North Rhyolite|43259|4|Described|Appendix 1,p6.||Early Carboniferous|||||||
24083|Watershed North Rhyolite|43589|2|Defined|p20|Early Carboniferous|Early Carboniferous|Comprises upper and lower units. Unconformably overlies Saint James Volcanics; unconformably overlain by Insolvency Gully Fm.  Intruded by Speed Creek Granite.||||||23-APR-08
24083|Watershed North Rhyolite|66529|5|Briefly described|p24 |Early Carboniferous|Early Carboniferous|Thought to have been deposited in a cauldron subsidence event.||||Unconformably overlies the Saint James Volcanics. Is overlain unconformably by Insolvency Gully Formation.|Crystal-rich to lithic-rich rhyolitic ignimbrite. At least 400m thick.|
24083|Watershed North Rhyolite|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Kennedy Province. Includes two unnamed subdivisions.|||||Mainly grey to dark grey, crystal-rich rhyolitic ignimbrite; mainly cream, moderately crystal- and clast-rich rhyolitic ignimbrite.|
24083|Watershed North Rhyolite|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Kennedy Province. Includes two informal subdivisions.|||||Mainly grey to dark grey, crystal-rich rhyolitic ignimbrite; mainly cream, moderately crystal- and clast-rich rhyolitic ignimbrite.|
24083|Watershed North Rhyolite|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba, Saint Giles and Tareela Volcanics; the Hells Gate, Oweenee, Paluma and Porcupine Creek Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
24083|Watershed North Rhyolite|69593|5|Briefly described|p494-496|Visean|Visean|Forms scattered outcrops in the Townsville region. May be included in the Oweenee Supersuite.|||||Thick sheets of crystal-rich to lithic-rich rhyolitic to dacitic ignimbrite; minor tuff, lava, breccia.|
69006|Wathonga Granite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|White to light grey, fine-grained, equigranular biotite leucogranite.||||||
69006|Wathonga Granite|65388|2|Defined|p335-336, p301 Fig 98, p340|Early Triassic|Late Permian|Of Tandora Suite. Appears as small windows in Tertiary sediments. Probably intrudes the Palaeozoic Yerilla Metamorphics under cover. Relationship to other granites not known.  All contacts concealed. Age uncertain. Mainly very light grey, fine to medium grained, equigranular biotite granite or leucogranite.||||||
69006|Wathonga Granite|68679|5|Briefly described|p419-420|||Rawbelle Batholith. ~2.5 km2; windows in Cenozoic cover. Relationship to nearby Carboniferous granites unknown. Geochemistry plot.||Tandora Suite.||Probably intrudes Yerilla Metamorphics.|Biotite leucogranite.|
30423|Watsonville Suite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Ootann Supersuite.||||||23-APR-09
30423|Watsonville Suite|60425|5|Briefly described|p280-1 Appdx. |Middle Permian|Middle Permian|Of Ootann Supersuite. Includes Watsonville Granite.  Age: ~281Ma, 289+/-16Ma (Rb-Sr). I-type.||||||07-FEB-11
40142|Wattlebank Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgwa].  Grey, fine to medium granodiorite, commonly xenolith-bearing; minor pink pegmatite.||||||
40142|Wattlebank Granodiorite|50209|5|Briefly described|Map Legend|Triassic|Permian|||||||
40142|Wattlebank Granodiorite|60557|5|Briefly described|p19 Fig. 5b|Late Triassic|Late Permian|Geochemically, part of the Clarence River Supersuite.  Hornblende-bearing I-type granitoid dominated by granodiorite, tonalite and quartz diorite.||||||09-JUN-05
40142|Wattlebank Granodiorite|65388|6|Mentioned|p70 Fig. 28|||Permian to Triassic? ||||||
40142|Wattlebank Granodiorite|68008|2|Defined|p174, p307, p334, p337-340, p393, p484|Permian|Permian|Newly defined in this study. Previously included as part of the Ridgelands Granodiorite by Kirkegaard et al. (1970). Separated on the bases of geophysics, geochemistry, geography and age. Several outcrops listed of a single 14 x 4 km pluton. The type area is in the vicinity of Wattlebank property after which the unit is named. Geochemistry described: very similar to Ridgelands Granodiorite.|269 Ma, 264 Ma (K-Ar hornblende; Webb, 1969).|||Intrudes Princhester Serpentinite.|The central part is a fairly uniform hornblende-biotite granodiorite. Around the margins the composition is tonalitic. Locally, large microgranodiorite boulders crop out. Local duricrust veneer. Lithologies described in some detail.|
40142|Wattlebank Granodiorite|68679|5|Briefly described|p308, p426-427|||Yarrol Province. 5 x 2.5 km unit straddling Fitzroy River and some smaller bodies; magnetic images indicate greater extent under alluvium. Geochemistry briefly described.|269 +/- 5 and 264 Ma (K-Ar: Webb, 1969).|||Intrudes Princhester Serpentinite, Mount Alma Formation.|Granodiorite; minor pink pegmatite.|
40142|Wattlebank Granodiorite|69952|6|Mentioned|p75|Early Triassic|Permian|||||||
23161|Weaner Vale Granite|23049|3|Fully described|p28|Early Devonian|Late Silurian|of Amarra Suite.||||||
23161|Weaner Vale Granite|23283|2|Defined|p22|Devonian|Silurian|||||||
23161|Weaner Vale Granite|23422|5|Briefly described|p216 Table 6.10|Early Devonian|Late Silurian|Of Amarra Supersuite.||||||
23161|Weaner Vale Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
23161|Weaner Vale Granite|69592|5|Briefly described|p293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~12 km2.||Amarra Suite.|||Grey to pink, medium-grained, rarely porphyritic biotite granite; intruded by numerous pegmatite dykes, and cut by abundant fractures filled by a dark alteration product (chloritic alteration?).|
24567|Welfern Granite|23220|6|Mentioned|Fig.2, p11|||of Forsayth Subprovince.||||||
24567|Welfern Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Parent: Forsayth Supersuite. Geological Province: Georgetown Region.||||||18-JUN-15
24567|Welfern Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 816. S-Type.||||||
24567|Welfern Granite|24197|5|Briefly described|p17, p79 tb. 9.1|Mesoproterozoic|Mesoproterozoic|Of the Forsayth Supersuite. Age: ~1550Ma. Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
24567|Welfern Granite|35920|2|Defined|p25|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24567|Welfern Granite|36937|6|Mentioned|p229|||||||||
24567|Welfern Granite|37570|4|Described|p121|||||||||
24567|Welfern Granite|37576|5|Briefly described|p8|||||||||
24567|Welfern Granite|39445|5|Briefly described|Table 2|||See also P72 & P148||||||
24567|Welfern Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24567|Welfern Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
24567|Welfern Granite|50211|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Pink to cream, foliated, medium-grained biotite leucogranite. Age: 1550-1560 Ma.||||||18-JUN-15
24567|Welfern Granite|50537|5|Briefly described|p1.2, 1.4, 2.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgetown Inlier. Of the Forsayth Supersuite.||||||
24567|Welfern Granite|68357|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Etheridge Province.|||||Pink to cream, foliated, medium-grained biotite leucogranite.|
24567|Welfern Granite|69591|6|Mentioned|p81, p83|Mesoproterozoic|Mesoproterozoic|Gilberton area. Although not part of the Forsayth Batholith, this unit probably belongs in the Forsayth Supersuite.||||||
79962|Werewilka Formation|71251|6|Mentioned|p3, p48|||Yowah-Cunnamulla area. Has a stripy magnetic domain. Map symbol suggests age inferred to be Cambrian.||||||26-APR-18
79962|Werewilka Formation|71864|6|Mentioned|p3|||||||||
79962|Werewilka Formation|71965|5|Briefly described|p896,899,901,903-906,908,910-911,913|Furongian|Late Cambrian|Geological province: Thomson Orogen. Marker unit through the southern Thomson Orogen and defines a broad fold with an E-W to NE-SW-trending axial planes and a faulted hinge marked by the Caiwarro fault zone; possible "on-strike" stratigraphic equivalent, and adjacent to Nebine Metamorphics. Observed as elongate domains of distinctly stripy magnetic appearance related to narrow parallel zones of alternating high and low magnetic character. Age constraints: c. 506 Ma (MDA); 455.6+\-2.4 Ma (intrusion).|c. 506 Ma (MDA)|||Laterally grades into Lycosa Formation and Thomson beds. Correlable with Warratta Group, Tongo Formation, Twin Tanks Metamorphics, Nebine Metamorphics.|Interbedded sandstone, siltstone and calc-silicates.|29-OCT-19
79962|Werewilka Formation|72915|6|Mentioned|p5|||Map symbol suggests Cambrian age.||||||
69681|Werite beds|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Geological region: Diamantina.||||||
69681|Werite beds|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit and the Edkins Formation are mapped under the symbol Ts: mostly unnamed sedimentary rocks.||||||
69681|Werite beds|69599|5|Briefly described|p580, p584, p600|Miocene|Paleocene|Vine (1964). Crops out on the escarpment and ranges SSE of Winton; forms the Forsyth Range, and caps the Allen and eastern Cory Ranges. 45m thick. Contains ferruginised flora of leaves and seeds. Capped by the Canaway profile.||||Unconformably overlies Winton Formation. Correlated (at least partly) with Moonie, Eyre, Glendower, Edkins, Springvale and Marion Formations; Old Cork beds; Mueller and Moses Sandstones.|Succession of quartz sandstone, silty sandstone, minor conglomerate and mudstone. Deeply lateritised surface: in turn, the beds are silicified and partly ferruginised.|
36431|West Creek Diorite|23617|3|Fully described|Table 2 p16||Early Permian|Intrudes Kangaroo Hills Fm. Is intruded by Poison Ck Granite. 293 Ma (SHRIMP). Also see p32. Type area proposed on the interfluve between West and Douglas Creek, about 7 km north-west of Boulder Mountain (8060-3603 79349). Kennedy Province.||||||
36431|West Creek Diorite|23618|5|Briefly described|map legend||Early Permian|||||||
36431|West Creek Diorite|69593|6|Mentioned|p495|Permian|Early Carboniferous|Ingham Batholith.||||||
41787|West Hill Granodiorite|60473|5|Briefly described|Map Legend|Tertiary|Tertiary|Dark grey to dark greenish grey, very fine grained, even grained to slightly porphyritic hornblende granodiorite.||||||
41787|West Hill Granodiorite|65388|3|Fully described|p423|Neogene|Paleogene|Intrudes the Campwyn Volcanics and is overlain by unconsolidated Cainozoic deposits. Age poorly constrained. Dark grey to locally dark greenish grey (altered), very fine-grained, slightly porphyritic hornblende granodiorite.||||||
36444|West Rishton Granodiorite|23430|5|Briefly described|Table 14.2 p460||Silurian|K-Ar; Rb-Sr age 411+/-2 Ma. Ravenswood Batholith||||||
38176|West Rishton Tonalite|23422|5|Briefly described|p176|Silurian|Silurian|Of Millchester Supersuite.||||||
36371|Western Creeks Cherty Shale Formation|23425|5|Briefly described|p373 Fig 9.10|||Of Pascoe River Group.||||||
27930|Westgrove Ironstone Member|13516|5|Briefly described|p159 fig 8, p172|Early Jurassic|Early Jurassic|From Surat Basin||Of Evergreen Formation||||
27930|Westgrove Ironstone Member|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
27930|Westgrove Ironstone Member|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
27930|Westgrove Ironstone Member|23799|5|Briefly described|p51, p52, p10 Tb. 1|Early Jurassic|Early Jurassic|Of Evergreen Fm. Max. thickness: ~50m.  Confined to eastern side of Mimosa Syncline in this pub., contrary to original placing on western side by Mollan and others (1965).  Geol. Prov: Surat Basin.||||||29-OCT-15
27930|Westgrove Ironstone Member|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Evergreen Formation.||||||
27930|Westgrove Ironstone Member|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
27930|Westgrove Ironstone Member|29960|5|Briefly described|p8|||Jurassic||||||
27930|Westgrove Ironstone Member|31116|4|Described|p21|||||||||
27930|Westgrove Ironstone Member|31118|6|Mentioned|p320|||||||||
27930|Westgrove Ironstone Member|32040|5|Briefly described|p886|||marine oolitic chamosite||||||
27930|Westgrove Ironstone Member|32136|4|Described|p3|||Persistent marker. Stratigraphy||||||
27930|Westgrove Ironstone Member|33381|6|Mentioned|p117|||L.Jur. Corr. Chart||||||
27930|Westgrove Ironstone Member|33672|6|Mentioned|p41|||||||||
27930|Westgrove Ironstone Member|33774|6|Mentioned|p48|||Stratigraphy||||||
27930|Westgrove Ironstone Member|34452|6|Mentioned|p1|||Evergreen Formation. See also PP19,21||||||
27930|Westgrove Ironstone Member|35095|6|Mentioned|p116|||||||||
27930|Westgrove Ironstone Member|35157|6|Mentioned|p523|||||||||
27930|Westgrove Ironstone Member|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
27930|Westgrove Ironstone Member|36111|6|Mentioned|p34|||||||||
27930|Westgrove Ironstone Member|37995|6|Mentioned|p62|||||||||
27930|Westgrove Ironstone Member|39212|4|Described|p36|||Excursion site||||||
27930|Westgrove Ironstone Member|40250|4|Described|p30|||||||||
27930|Westgrove Ironstone Member|40541|4|Described|p108|||||||||
27930|Westgrove Ironstone Member|40666|4|Described|p356|||||||||
27930|Westgrove Ironstone Member|41210|6|Mentioned|p158|||||||||
27930|Westgrove Ironstone Member|41747|6|Mentioned|p471|||||||||
27930|Westgrove Ironstone Member|42911|5|Briefly described|p13|||Of Evergreen Formation||||||16-SEP-08
27930|Westgrove Ironstone Member|43000|5|Briefly described|Fig.5,p112|||Of Evergreen Formation.||||||16-SEP-08
27930|Westgrove Ironstone Member|43185|5|Briefly described|6||Jurassic|||||||
27930|Westgrove Ironstone Member|43714|6|Mentioned|Fig.3,p5||Early Jurassic|||||||
27930|Westgrove Ironstone Member|43982|14|Not recorded|Map Legend|||||||||
27930|Westgrove Ironstone Member|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
27930|Westgrove Ironstone Member|43994|14|Not recorded|Map Legend||Jurassic|||||||
27930|Westgrove Ironstone Member|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
27930|Westgrove Ironstone Member|44023|4|Described|Tb.3,p10-11||Early Jurassic|||||||
27930|Westgrove Ironstone Member|44032|14|Not recorded|p462,464|||Part of Evergreen Formation.||||||
27930|Westgrove Ironstone Member|44174|14|Not recorded|p345,347,348||Early Jurassic|Member of Evergreen Formation||||||
27930|Westgrove Ironstone Member|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
27930|Westgrove Ironstone Member|44390|14|Not recorded|p9,16,Tb.1||Early Jurassic|||||||
27930|Westgrove Ironstone Member|44391|14|Not recorded|Map Legend||Early Jurassic|Part of Evergreen Formation.||||||
27930|Westgrove Ironstone Member|44420|14|Not recorded|p26,29,Appendix 1|||Ref. to Jensen et al. 1964.||||||
27930|Westgrove Ironstone Member|44421|14|Not recorded|p11-14||Jurassic|||||||
27930|Westgrove Ironstone Member|44636|14|Not recorded|p166|||=Upper Evergreen.||||||
27930|Westgrove Ironstone Member|45071|3|Fully described|Table 15|||||||||
27930|Westgrove Ironstone Member|45110|3|Fully described|p91|||See also p63 and p90.||||||16-NOV-15
27930|Westgrove Ironstone Member|48900|4|Described|p51|||||||||
27930|Westgrove Ironstone Member|48919|4|Described|p45|||Jurassic. See also p46-53.||||||16-NOV-15
27930|Westgrove Ironstone Member|48920|6|Mentioned|p90|||||||||
27930|Westgrove Ironstone Member|60998|5|Briefly described|p145|||Of Mollan et al  (1972). ||||||
27930|Westgrove Ironstone Member|60999|5|Briefly described|p177|||Oolitic beds within the Evergreen Formation. Geological Province: Surat Basin.||||||
27930|Westgrove Ironstone Member|63218|6|Mentioned|p211 Fig.2. |Early Jurassic|Early Jurassic|Surat Basin.||Unit in Evergreen Formation.||||
27930|Westgrove Ironstone Member|63979|5|Briefly described|p33|Toarcian|Toarcian|Oolitic unit in the Evergreen Formation.||||||07-FEB-11
27930|Westgrove Ironstone Member|64665|5|Briefly described|p53 Fig.2.|Early Jurassic|Early Jurassic|Surat Basin.||Unit in Evergreen Formation.||||
27930|Westgrove Ironstone Member|64856|4|Described|p79, p82-85|Toarcian|Toarcian|Mollan et al. (1965). Surat Basin. An oolitic Member contained in the upper portion of the Evergreen Formation on the western side of the Mimosa Syncline. Age from palynoflora unit APJ32 (175.6-178 Ma).| | ||||29-NOV-17
27930|Westgrove Ironstone Member|64857|5|Briefly described|p130-132, p113 Fig.3|||Uppermost member of the Evergreen Formation. Surat Basin. Dense black mudstones.||||||
27930|Westgrove Ironstone Member|65117|4|Described|p467, 468-469, fig 4 p465, Tbl 1 p466|Toarcian|Toarcian|Of Evergreen Formation, Surat Basin. Overlies, and is more extensive than, the Boxvale Sandstone Member. Deposited in a lacustrine delta environment.||||||
27930|Westgrove Ironstone Member|65388|5|Briefly described|p211|||Of Mollan & others (1965).  Mulgildie Basin, Surat Basin. 3-9m thick. Mudstone, siltstone and sandstone containing an oolitic member at its base.||||||
27930|Westgrove Ironstone Member|66915|5|Briefly described|p6 Fig.3|Early Jurassic|Early Jurassic|Surat Basin.||||||
27930|Westgrove Ironstone Member|67133|5|Briefly described|p11|Jurassic|Jurassic|Demonstrates a shift towards a marine-influenced delta depositional system, possibly without connection to the sea. Appears only as Westgrove Ironstone.||Evergreen Formation.|||Oolitic mudstones and sideritic cement.|
27930|Westgrove Ironstone Member|68117|5|Briefly described|p346|Early Jurassic|Early Jurassic|Surat Basin.||Evergreen Formation.||||
27930|Westgrove Ironstone Member|68139|6|Mentioned|p23|Early Jurassic|Early Jurassic|Surat Basin.||Evergreen Formation.||||
27930|Westgrove Ironstone Member|68576|5|Briefly described|Q_4: p3, p22|Early Jurassic|Early Jurassic|Surat Basin. Possibly deposited under shallow-marine conditions.||Evergreen Formation.|||Interbedded mudstone and chamositic mudstone with pelletal or oolitic structure with sideritic cement and minor labile sandstone.|
27930|Westgrove Ironstone Member|69594|4|Described|p519, p535, p536 Fig.7.17, p546|||Mollan et al. (1965). Northern Surat Basin. Shallow-marine or non-marine lacustrine deposits.||Evergreen Formation.||Overlies Boxvale Sandstone Member. Age-equivalent of Brighton beds, Ma Ma Creek Member and Tiaro Coal Measures.|Interbedded mudstone, chamositic mudstone which is pelletal or oolitic, and minor sandstone.|
27930|Westgrove Ironstone Member|69633|4|Described|p1, p3-8, p10 Fig.6, p11-12, p14-15, p20|Early Jurassic|Early Jurassic|Ubiquitous throughout Surat Basin. Widespread lacustrine deposition was synchronous across the Nambour, Clarence-Moreton and Surat Basins. GSQ Chinchilla 4 core log detailed. Palynology detailed. Sections from well completion reports are included in Appendix 3.||Evergreen Formation.||Overlies Boxvale Sandstone Member.|Reddish-brown massive ironstone, characterised by authigenic siderite precipitates.|
27930|Westgrove Ironstone Member|69681|6|Mentioned|p74 Fig.3|Early Jurassic|Early Jurassic|||||||
27930|Westgrove Ironstone Member|69682|5|Briefly described|p94|Early Jurassic|Early Jurassic|Surat Basin.||Unit in Evergreen Formation.||||
27930|Westgrove Ironstone Member|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Surat Basin.||Unit in Evergreen Formation.||||
27930|Westgrove Ironstone Member|71805|5|Briefly described|p77, p79|||Surat Basin. Interpreted to have been deposited in a fresh-water lacustrine environment.||Evergreen Formation||||15-MAY-19
27930|Westgrove Ironstone Member|71806|5|Briefly described|p483, p485|||Surat Basin. Features chamositic oolite layers.||Evergreen Formation.||Overlies the Boxvale Sandstone Member.||
27930|Westgrove Ironstone Member|72921|5|Briefly described|p15 Fig.2, p16.|Early Jurassic|Early Jurassic|Interpreted as correlative across the Clarence-Moreton, Surat and Eromanga Basins. Said to be part of Evergreen Formation, but appears to be shown as part of Koukandowie Formation as well, in Fig.2.||Evergreen Formation||||
27930|Westgrove Ironstone Member|73147|5|Briefly described|p127|Early Jurassic|Early Jurassic|Marks a rapid, short-lived, westward marine incursion into the Great Australian Superbasin.||Evergreen Formation.||||
27930|Westgrove Ironstone Member|73393|6|Mentioned|p19-23|Toarcian|Toarcian|Surat Basin. An almost complete Jurassic tetrapod amphibian, Siderops kehli, was recovered from this unit (Kolane cattle station, SE QLD) along with two partially articulated freshwater plesiosaur specimens. Detrital zircons collected alongside the fossil specimens yielded a maximum depositional age of 176.6 +/- 2.0 Ma.||Evergreen Formation|||Oolitic ironstone.|
27930|Westgrove Ironstone Member|73600|6|Mentioned|191|Toarcian|Toarcian|||Evergreen Formation||Underlain by Boxvale Sandstone Member.||
78570|Weston beds|68731|6|Mentioned|p199, p200 Fig 3.110|Wordian|Roadian|Price et al. (1985); Price (1997). Galilee Basin.||||Unconformably overlain by the Betts Creek beds. Unconformably underlain by the Aramac Coal Measures.||19-DEC-13
78570|Weston beds|72088|5|Briefly described|p8, p91|Wordian|Roadian|Lovelle Depression, Galileee Basin.||||Unconformably overlies the Aramac Coal Measures. Unconformably overlain by the Betts Creek beds.||
78570|Weston beds|73472|6|Mentioned|p115|Wordian|Roadian|Galilee Basin, Lovelle Depression.||||||
36387|Weymouth Supersuite|23420|4|Described|p 147 table 4.6|Permian|Late Carboniferous|Also see p 130. Age: 285Ma||||||
36387|Weymouth Supersuite|23431|5|Briefly described|p536|||I-Type granite.||||||
36387|Weymouth Supersuite|63154|5|Briefly described|p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Coen Inlier.||||||
36387|Weymouth Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Brodies Camp, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
36387|Weymouth Supersuite|69593|4|Described|p475-477, p512|Permian|Late Carboniferous|Knutson, Bultitude and Sun (1994). High-level granitoids in the northern Coen region (Jardine Subprovince, Kennedy Igneous Association). Rhyolitic-dacitic rocks of the Janet Ranges Volcanic Group are tentatively included in this unit. Associated with Sn (mostly alluvial), W-Mo-Bi and some Au mineralisation. Sm-Nd isotope data tabulated.|||Twin Humps, Wigan, Wolverton Adamellites; Weymouth, Portland Roads Granites; see COMMENTS.||I-type; (allanite-)hornblende-biotite and (allanite-)biotite-hornblende granodiorite and biotite monzogranite. Dioritic enclaves to 30cm relatively common. Pyroxene-hornblende and biotite-hornblende diorite may be related.|
36387|Weymouth Supersuite|71792|5|Briefly described|p9, p13, p25, p31|Early Permian|Early Permian|Exposed in the Cape Weymouth 1:250k map sheet where granitoids are emplaced at relatively shallow levels. An additional SHRIMP age, also derived from Black et al is 284 +/- 4 Ma.|287 +/- 8 Ma (U-Pb SHRIMP Black et al, 1992a & b)||Includes the Twin Humps Granite, Wigan Granite, Lockhart River Granite.|Intrudes the Choc-a-Block Orthogneiss.|Granitoids.|
36387|Weymouth Supersuite|71849|4|Described|p2, p4-5, p8, p10, p12, p51, p57, p79|Permian|Permian|See also p126, p130-132, p144, p179-183, p185-186, p195. Coen Inlier. Greatest compositional range of all the Supersuites in the region. Geochemistry detailed. Emplaced at relatively shallow crustal levels. Contains auriferous veins in the north; small-scale mining in the past. See constituents for ages.|c.284-288 Ma.||Wolverton, Twin Humps Granites.|Intrudes Buthen Buthen Granite.|I-type.|
36387|Weymouth Supersuite|71853|5|Briefly described|Map legend.|Permian|Permian||||Wolverton, Weymouth, Lockhart River Granites.|||
36387|Weymouth Supersuite|71854|5|Briefly described|Map legend.|Permian|Permian||||Wolverton, Weymouth, Twin Humps Granites.|||
36387|Weymouth Supersuite|72983|6|Mentioned|p60||||||Weymouth Granite, Twin Humps Granite|||
24569|Wheatley Oil Shale Member|40247|5|Briefly described|p211|||||||||
24569|Wheatley Oil Shale Member|40954|6|Mentioned|p133|||||||||
24569|Wheatley Oil Shale Member|68319|5|Briefly described|Map Legend|Eocene|Eocene|||Of the Lowmead Formation||Conformably overlain by the Korenan Oil Shale Member. Conformably underlain by the Harpur Creek Member.|Brownish black, carbonaceous oil shale, minor interbedded olive-grey claystone.|
24569|Wheatley Oil Shale Member|68421|5|Briefly described|Map Legend|Eocene|Eocene|Lowmead Graben.||Of the Lowmead Formation.||Conformably overlain by the Korenan Oil Shale Member. Conformably underlain by the Harpur Creek Member.|Brownish black, carbonaceous oil shale; minor interbedded olive-grey claystone.|
24569|Wheatley Oil Shale Member|69599|5|Briefly described|p588|Paleogene|Paleogene|McConnochie and Henstridge (1985). Lowmead Graben. 14.3 - 41.7m thick, averaging 25.4m.||Lowmead Formation.||Overlies Harpur Creek Member. Is overlain by Korenan Oil Shale Member.|Carbonaceous oil shale, minor interbedded claystone.|
75130|Wheeler Suite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of the Wheeler Supersuite. Contains the Wheeler granite (informally named). A-type.||||||07-FEB-11
75131|Wheeler Supersuite|60425|5|Briefly described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Contains the Wheeler Suite. A-type.||||||07-FEB-11
75129|Wheeler granite|60425|4|Described|p98, p100, p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of Wheeler Suite (Wheeler Supersuite).Informal name for granite on Wheeler Island.In Bedarra Granite Belt. Med.gr, slightly porphyritic biotite granite; + scattered feldpsar phenocrysts to ~2cm; heterogeneous with biotite-rich zones; A-type + more detail.||||||07-FEB-11
36264|Whelan Creek Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36264|Whelan Creek Granite|60425|5|Briefly described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Grey biotite granite - originally informally referred to as Deadman granite, but name subsequently used by Mackenzie et al (1993) for another unit. I-type.||||||07-FEB-11
41780|Whelan Creek Volcanics|60445|5|Briefly described|p5|Late Carboniferous|Late Carboniferous|Of the Connors Volcanic Group. Series of massive crystal-rich, generally lithic-poor, locally fiamme-bearing rhyolitic ignimbrite sheets and aphyric to sparsely porphyritic rhyolite lava flows and high level intrusives.||||||
41780|Whelan Creek Volcanics|60472|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich, generally lithic poor, locally fiamme-bearing, rhyolitic ignimbrite; rhyolite flows and high level intrusives.||||||
41780|Whelan Creek Volcanics|60473|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich, generally lithics-poor, locally fiamme-bearing rhyolitic ignimbrite and aphyric to sparsely porphyritic rhyolite lava flows and high level intrusives.||||||29-SEP-04
41780|Whelan Creek Volcanics|60475|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Crystal rich, generally lithic poor, locally fiamme-bearing, rhyolitic ignimbrite; aphyric to sparsely porphyritic rhyolite flows and high level intrusives.||||||
41780|Whelan Creek Volcanics|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Crystal rich, generally lithic poor, locally fiamme bearing, rhyolitic ignimbrite; aphyric to sparsely porphyritic rhyolite flows and high level intrusives.||||||
41780|Whelan Creek Volcanics|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
41780|Whelan Creek Volcanics|65388|4|Described|p96-98, 97, 59, 84, 85, 90, 92, 94|Late Carboniferous|Late Carboniferous|Of Connors Volcanic Group, Connors Arch.  Overlie the Mountain View Volcanics at least disconformably; overlain by conglomerate tentatively assigned to the Carmila beds and by Leura Volcanics. Intruded by Dacey Granite and Toobier Granite. SHRIMP ages: 314.1+/-5 Ma, 317.7+/-5.6 Ma. Dominated by massive, generally dark grey, crystal-lithic rhyolitic to dacitic ignimbrite sheets. See also p110, 135, 360, 362, 447.||||||
41780|Whelan Creek Volcanics|68679|4|Described|p355-356, p362|Pennsylvanian|Pennsylvanian|See also reference to Mount Whelan Volcanics (p353). May be coeval with the Broadsound Range Volcanics.|314.1 +/- 5.0 Ma (SHRIMP: Fanning et al., 2009).|Connors Volcanic Group.||Overlies Mountain View Volcanics. Is intruded by the Dacey and Toobier Granites.|Dominated by thick sheets of crystal-lithic rhyolitic to dacitic ignimbrite, with locally interbedded lithic sandstone and thinly laminated very fine volcaniclastic siltstone.|
41780|Whelan Creek Volcanics|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|||||Ignimbrite.|
69504|Whiphole Spring Granite|68350|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Cream, fine- to coarse-grained, equigranular to porphyritic biotite granite.|
69504|Whiphole Spring Granite|68351|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province. Unit in Oweenee Batholith.|||||Cream, fine- to coarse-grained, equigranular to porphyritic biotite granite.|
36625|Whippole Creek trondhjemite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 478.  I-Type.||||||
36221|Whistler Granite|23291|5|Briefly described|p102 Tb. 3.13|Late Carboniferous|Late Carboniferous|Parent: Rocky Whistler Suite. Early phase of Tate Batholith. Geological Province: Georgetown Region.||||||08-JUL-15
36221|Whistler Granite|23502|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
36221|Whistler Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 368. I-Type.||||||
36221|Whistler Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
36221|Whistler Granite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Fine- to medium-grained, porphyritic (muscovite-)biotite monzogranite.|
36221|Whistler Granite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Fine- to medium-grained, porphyritic (muscovite-)biotite monzogranite.|
36221|Whistler Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the Ootann Supersuite.|||Fine to medium-grained, porphyritic (muscovite-) biotite granite.|
27254|White Blow Formation|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Albert Group. Overlies the Deighton Quartzite.||||||17-DEC-07
27254|White Blow Formation|30531|6|Mentioned|p20|||Also mention Fig.2.||||||
27254|White Blow Formation|30532|2|Defined|p113|Precambrian|Precambrian|||||||
27254|White Blow Formation|32660|5|Briefly described|Table 5|||||||||
27254|White Blow Formation|32959|6|Mentioned|Fig.21|||||||||
27254|White Blow Formation|33900|5|Briefly described|p18|||Mention p15.||||||15-FEB-17
27254|White Blow Formation|35074|6|Mentioned|Fig.2|||||||||
27254|White Blow Formation|35286|6|Mentioned|Fig.17|||||||||
27254|White Blow Formation|36052|6|Mentioned|Fig.2|||||||||
27254|White Blow Formation|37868|5|Briefly described|p207|||||||||
27254|White Blow Formation|39445|5|Briefly described|Table 2|||See also P42 & P43||||||
27254|White Blow Formation|39492|6|Mentioned|p30|||||||||
27254|White Blow Formation|39622|6|Mentioned|Fig.2|||||||||
27254|White Blow Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27254|White Blow Formation|39937|6|Mentioned|Fig.1|||||||||
27254|White Blow Formation|40840|6|Mentioned|Map legend|||||||||
27254|White Blow Formation|40984|4|Described|p389|||||||||
27254|White Blow Formation|41744|5|Briefly described|p406|||||||||
27254|White Blow Formation|42565|6|Mentioned|p2|||||||||
27254|White Blow Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mount Albert Group. Pelitic and calcareous sedimentary rocks.||||||09-FEB-09
27254|White Blow Formation|45136|3|Fully described|p43|||||||||
27254|White Blow Formation|45166|4|Described|p32|||||||||
27254|White Blow Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
27254|White Blow Formation|46960|6|Mentioned|p221|||||||||
27254|White Blow Formation|50332|6|Mentioned|p16, p89|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma.||||||07-FEB-11
27254|White Blow Formation|62047|6|Mentioned|p90 Fig.1  |||||||||
27254|White Blow Formation|64248|6|Mentioned|p38 Fig.5|||||Mount Albert Group||Overlies Deighton Quartzite.||
27254|White Blow Formation|64249|6|Mentioned|p85|||Geological Province: Mount Isa Inlier.||||||22-APR-09
27254|White Blow Formation|64250|5|Briefly described|p13 fig 5, p11 fig 3, p18|||Kalkadoon-Leichhardt Belt, Mount Isa Inlier.||Mount Albert Group.||Overlies Deighton Quartzite (mostly conformably).|Pelitic and calcareous rocks.|
27254|White Blow Formation|65396|5|Briefly described|p7, p11 Fig.6, p16-17, p82, p84, p103|Calymmian|Statherian|See also p121, p143, p160, p175, p182-184, p190, p241. Kalkadoon-Leichhardt Belt. Has striking similarities with the underlying Deighton Quartzite.||Mount Albert Group||Conformably (locally unconformably) overlies Deighton Quartzite.|Pelitic and calcareous rocks, including staurolite-garnet schist.|
27254|White Blow Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p15|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Calvert Superbasin.||Mount Albert Group.||Unconformably overlies the Corella Formation.|Metasiltstone, phyllite, garnet, staurolite and andalusite schist|
27254|White Blow Formation|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian||1728 +/- 5 Ma max detrital SHRIMP age.|Lower Mount Albert Group.||||16-MAR-18
27254|White Blow Formation|69591|5|Briefly described|p56|||Mary Kathleen Domain, Mount Isa Province. Part of Prize and Gun Supersequences. Deep marine sediments.|||||Metasiltstone, phyllite, garnet, staurolite and andalusite schist.|
27254|White Blow Formation|72297|6|Mentioned|p721, p759|||Eastern Fold Belt of the Mount Isa Inlier. Contains abundant staurolite as twinned crystals (Maltese crosses) near the Wee MacGregor mine, SW of Cloncurry.||||||
27254|White Blow Formation|73525|6|Mentioned|p4-5 Fig.2|||Kalkadoon-Leichhardt River Domain.|||||Felsic extrusives.|
27254|White Blow Formation|73529|6|Mentioned|p5|||Calvert Superbasin, late. Deep marine setting.||Mount Albert Group||||
27254|White Blow Formation|73553|6|Mentioned|p8 Fig.1.2.3, p187|||||Mount Albert Group||||
24571|White Bull Member|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon). Thickness: 100-300m. Geological Province: Georgetown Region.||||||08-JUL-15
24571|White Bull Member|35921|2|Defined|p40|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24571|White Bull Member|36937|6|Mentioned|p229|||||||||
24571|White Bull Member|37570|6|Mentioned|p125|||||||||
24571|White Bull Member|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24571|White Bull Member|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24571|White Bull Member|41975|5|Briefly described|Table 1 P434|||||||||
24571|White Bull Member|43664|4|Described|p31|||||||||
24571|White Bull Member|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Candlow Formation.||||||07-NOV-08
24571|White Bull Member|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||
24571|White Bull Member|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Candlow Formation. Mudstone, siltstone, sandstone.||||||07-NOV-08
24571|White Bull Member|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Candlow Formation (Etheridge Group).  Siliceous/quartzose siltstone, fine sandstone, variably carbonaceous mudstone and siltstone.||||||06-JUL-04
24571|White Bull Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||Candlow Formation.||||
24571|White Bull Member|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|08-JUL-15
24571|White Bull Member|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|13-MAY-15
24571|White Bull Member|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Mudstone, siltstone, and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|13-MAY-15
24571|White Bull Member|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Candlow Formation.|||Mudstone, siltstone and mudclast sandstone; conspicuous dark grey quartzose siltstone to fine sandstone.|
23187|White Crystal Granite|23424|5|Briefly described|p339|||Of Oweenee Supersuite, Ingham Batholith.||||||
23187|White Crystal Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 137. I-Type.||||||
23187|White Crystal Granite|23617|4|Described|Table 2 p18|||Possibly intrudes Poison Creek Granite. Also see p24 + Table 3 p52. K-Ar 324 +/- 10 Ma. Of Oweenee Supersuite of Kennedy Province.||||||
23187|White Crystal Granite|23618|5|Briefly described|map legend||Carboniferous|||||||
23187|White Crystal Granite|43259|4|Described|Appendix 1,p25.||Carboniferous|||||||
23187|White Crystal Granite|69593|5|Briefly described|p494||||~345-330 Ma.|Oweenee Supersuite.||||
29274|White Springs Granodiorite|9539|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Grey porphyritic muscovite-biotite leucogranite and granodiorite.||||||
29274|White Springs Granodiorite|23291|5|Briefly described|p35, p89 Tb. 3.8|Silurian|Silurian|Age: 424+/-11Ma. Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||29-MAY-15
29274|White Springs Granodiorite|23429|5|Briefly described|p434 Fig 13.2|||||||||
29274|White Springs Granodiorite|23430|5|Briefly described|Table 14.2 p460.||Devonian|K-Ar; Rb-Sr 404-407 Ma. Zircon crystallisation (424 +/- 11 Ma). Pama Province.||||||29-MAY-15
29274|White Springs Granodiorite|23453|5|Briefly described|p14|Early Devonian|Late Silurian|||||||
29274|White Springs Granodiorite|23619|5|Briefly described|p7|||||||||
29274|White Springs Granodiorite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29274|White Springs Granodiorite|33909|2|Defined|p230|Proterozoic|Proterozoic|||||||
29274|White Springs Granodiorite|35214|6|Mentioned|p7|||||||||
29274|White Springs Granodiorite|36153|6|Mentioned|Table 2|||||||||
29274|White Springs Granodiorite|37570|4|Described|p119|||||||||
29274|White Springs Granodiorite|39445|5|Briefly described|Table 2|||See also P45||||||
29274|White Springs Granodiorite|39687|6|Mentioned|p3|||||||||
29274|White Springs Granodiorite|39689|6|Mentioned|Fig.2|||||||||
29274|White Springs Granodiorite|39917|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
29274|White Springs Granodiorite|39981|6|Mentioned|p105|||||||||
29274|White Springs Granodiorite|41675|5|Briefly described|p66|||||||||
29274|White Springs Granodiorite|41680|6|Mentioned|p104|||||||||
29274|White Springs Granodiorite|43113|5|Briefly described|p7|||||||||
29274|White Springs Granodiorite|43259|4|Described|Appendix 1,p16.|Early Devonian|Late Silurian|||||||
29274|White Springs Granodiorite|43664|6|Mentioned|p94|||||||||
29274|White Springs Granodiorite|50198|5|Briefly described|Map Legend|Silurian|Silurian|||||||
29274|White Springs Granodiorite|68354|5|Briefly described|Map legend.|Silurian|Silurian|White Springs Batholith. Five facies are mapped separately.|||||Grey, medium-grained biotite granodiorite; sometimes porphyritic with equant K-feldspar phenocrysts/megacrysts; biotite-hornblende tonalite; cream muscovite leucogranite, aplite and pegmatite.|
29274|White Springs Granodiorite|68576|5|Briefly described|Q_11: p21-24|Silurian|Silurian|Is in contact with Einasleigh Metamorphics at O'Brien's Creek, but the nature of the contact is not specified.||White Springs Supersuite.|||Grey, medium-grained, equigranular to porphyritic muscovite-biotite and biotite granodiorite. Metaluminous to mildly peraluminous; I-type.|
29274|White Springs Granodiorite|69592|5|Briefly described|p281-282, p285|||Geochemistry plots. Other, similar ages given.|424 +/- 8 Ma (SHRIMP U-Pb zircon).|White Springs Supersuite.||||
29274|White Springs Granodiorite|71592|5|Briefly described|Appendix A.||||424+/-11 Ma (SHRIMP U-Pb zircon).||||Granodiorite.|
36107|White Springs Supersuite|23291|4|Described|p35, p89 Tb. 3.8|Devonian|Silurian|Age range: 424+/-11Ma to >390Ma. Intrudes Etheridge Group, McDevitt and Dargalong Metamorphics. Geological Province: Georgetown Region.||||||08-JUL-15
36107|White Springs Supersuite|23500|6|Mentioned|Map legend|Early Silurian|Late Ordovician|||||||
36107|White Springs Supersuite|23501|6|Mentioned|map legend|Early Silurian|Late Ordovician|Shown as White Springs (Blackman Gap) Supersuite. What does this mean? Both terms seem to be current.||||||
36107|White Springs Supersuite|23502|5|Briefly described|Map Legend|Early Silurian|Paleoproterozoic|Replaces Blackman Gap Supersuite? Shown as White Springs (Blackman Gap) Supersuite.||||||07-NOV-08
36107|White Springs Supersuite|23510|5|Briefly described|Map Legend||Silurian|||||||
36107|White Springs Supersuite|24485|6|Mentioned|p61 Tb.10|||||||||
36107|White Springs Supersuite|24486|5|Briefly described|Map legend|Early Silurian|Late Ordovician|||||||
36107|White Springs Supersuite|63154|5|Briefly described|p285 Fig. 5|Silurian|Silurian|Geological province: Georgetown Inlier. Mainly I-type granites.||||||11-APR-07
36107|White Springs Supersuite|67848|5|Briefly described|p8.|Late Silurian|Late Silurian|Georgetown Province. Granitoids.|<431 Ma (Bain and Draper 1997).|||||
36107|White Springs Supersuite|68330|5|Briefly described|Map legend.|Early Silurian|Early Silurian|Pama Province.|||Includes Blackman Gap Complex.|||
36107|White Springs Supersuite|68331|5|Briefly described|Map legend.|Early Silurian|Early Silurian|Pama Province.|||Includes Blackman Gap Complex.|||
36107|White Springs Supersuite|68337|5|Briefly described|Map legend|Early Silurian|Early Silurian|Written as White Springs (Blackman Gap) Supersuite. [White Springs Supersuite presumably supersedes Blackman Gap Supersuite].|||Includes Nundah Granodiorite.|||17-AUG-15
36107|White Springs Supersuite|68405|5|Briefly described|Map Legend|Early Silurian|Early Silurian|Pama Province.|||Includes Blackman Gap Complex, Bullock Creek Granite.|||
36107|White Springs Supersuite|68553|6|Mentioned|Map legend|Middle Devonian|Silurian|Etheridge Province. This unit, the Mount Webster and Dido Supersuites, and various ungrouped Silurian plutonic units, are all mapped under the same symbol, Sg.||||||
36107|White Springs Supersuite|68576|5|Briefly described|Q_11: p21|Silurian|Silurian|The dominant Silurian-Devonian granite Supersuite in the Georgetown region. Part of the Pama Igneous Association.|c.426 Ma.||White Springs Granodiorite.|||
36107|White Springs Supersuite|69591|5|Briefly described|p80|Silurian|Silurian|Forsayth Batholith.|||||Includes small plutons of granodiorite.|
36107|White Springs Supersuite|69592|5|Briefly described|p280-285, p288-291, p297|Silurian|Silurian|Georgetown Inlier. Geochemistry described in some detail; contrasted with the Toms Hole Supersuite. Includes most of the Pama Igneous Association granitoids. Crustal evolution discussed. CONSTITUENTS continued: Blackman Gap Complex; Jape Creek, Loafers, Nundah, Oak River, Puppy Camp, Robin Hood, White Springs Granodiorites.|c.424 Ma.||Anning, Beverly Hills, Bullock Creek, Cope, Dry Bore, Dumbano, Eleven-B, Ellendale, McKinnons Creek, Mount Juliet, Mount Misery, Quinine Spring, Skeleton Creek, Van Lee Granites. More in COMMENTS.||I-type. Variably porphyritic to even-grained biotite granodiorite, muscovite-biotite granite and granodiorite and biotite granite; biotite and biotite-hornblende tonalite to granodiorite; porphyritic biotite leucogranite.|
36107|White Springs Supersuite|70207|6|Mentioned|p73|||||||||
36107|White Springs Supersuite|71849|5|Briefly described|p173-176|Devonian|Silurian|Georgetown region. Geochemistry discussed in contrast with Flyspeck and Blue Mountains Supersuites.|||||I-type granitoids.|
35181|Whitehorse Granite|23042|4|Described|p82,3 Fig2||Late Carboniferous|||||||
35181|Whitehorse Granite|60472|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Urannah Batholith. Pink, medium grained, porphyritic biotite granite.||||||
35181|Whitehorse Granite|60473|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Urannah Batholith.  Pink, medium grained, porphyritic biotite granite.||||||
35181|Whitehorse Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35181|Whitehorse Granite|61917|5|Briefly described|Map legend|Early Permian|Early Permian|Pink, medium-grained, porphyritic biotite monzogranite to syenogranite; granophyric intergrowths common locally; cut by pegmatite, aplite and mafic dykes.||||||
35181|Whitehorse Granite|65388|2|Defined|p391-392, 135, 362, 364, 365,383,396,399|Early Permian|Early Permian|Northern Connors Arch. Southern Urannah Batholith. Intrudes Strathdee Granodiorite. SHRIMP age: ~285+/-2 Ma. Most commonly a pale pink, medium to coarse-grained, seriate biotite granite. Unnamed felsic dyke similar age.||||||
35181|Whitehorse Granite|68679|5|Briefly described|p361|Permian|Permian|Southern Connors Subprovince. Pennsylvanian-early Permian.|285.0+/-3.7 Ma: U-Pb SHRIMP: Fanning et al.(2009)|||||
35181|Whitehorse Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|285+/-3.7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
80682|Whites Creek Granodiorite|71849|3|Fully described|p3, p8, p13, p57-61, p87, p89, p150|Devonian|Devonian|See also p152-154, p162, p195. New name, after the abandoned Whites Creek prospect. Previously mapped partly as Kintore Adamellite and partly as Coen Metamorphics by Willmott et al. (1973) and Whitaker and Gibson (1977). An elongate, NNW-aligned pluton c.10 x c.3.5 km, ~18km W of Coen. Designated type area is around MGA 720851 8455756. Not mapped in detail. Forms undulating country, extremely weathered and very poorly exposed. Distinguishing geophysics, geochemistry described. Member of the Pama Igneous Association. Age is probable; not isotopically dated.||Buthen Buthen Suite.||Intrudes Coen Metamorphic Group. Adjacent to, and intruded by, Vardon Granite.|Grey, fine- to medium-grained, uneven-grained muscovite-biotite granodiorite. Only slightly altered, but moderately-extensively deformed. Inclusions of quartz, banded migmatitic gneiss and black quartzite up to ~1m, and biotite schist to ~5m. S-type.|
80682|Whites Creek Granodiorite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Buthen Buthen Suite.|||Grey, fine- to medium-grained, uneven-grained muscovite-biotite granodiorite.|
79367|Whitestone Creek Dacite|70740|5|Briefly described|i, iv, p72, p82 fig 50, p83,|Early Permian|Early Permian|Drummond Basin. The name is derived from Whitestone Creek, a tributary of the Rosetta Creek. Outcrop characteristics is discussed. 80-100m thick. A type locality is mentioned and described very briefly. Lithology and petrography is discussed in detail. May be early Permian in age. See also p87, p92-p95, p116.||Bulgonunna Volcanic Group||Unconformably overlies the Bimurra Volcanics. Conformably overlies the Conway Volcanics. Underlies Bobby Dazzler Rhyolite. Probably overlies Bungobine Rhyolite.|Crystal-rich, strongly welded dacitic ignimbrite.|08-JAN-21
79367|Whitestone Creek Dacite|73035|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Light brown to grey, very crystal-rich (plagioclase+hornblende+clinopyroxene+quartz), strongly welded dacitic ignimbrite.|
23190|Whitewater Creek Granite|23291|5|Briefly described|p99 Tb. 3.11, p101 Tb. 3.12|Late Carboniferous|Carboniferous|Probably of the Western Ingham Batholith (Cashmere area). Intrudes Etheridge Group. Underlies Undara Basalt. Geological Province: Georgetown Region.||||||08-JUL-15
23190|Whitewater Creek Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 420. I-Type.||||||
23190|Whitewater Creek Granite|23619|4|Described|p39 Table 2||Carboniferous|Intrudes Einasleigh Metamorphics. Overlain by McBride Basalt Group - unconformably.||||||14-NOV-06
23190|Whitewater Creek Granite|43113|4|Described|Table 2 p25||Carboniferous|||||||
23190|Whitewater Creek Granite|43253|5|Briefly described|map legend||Carboniferous|||||||
23190|Whitewater Creek Granite|43259|4|Described|Appendix 1,p46.||Carboniferous|||||||
23190|Whitewater Creek Granite|43716|6|Mentioned|p17|||||||||
23190|Whitewater Creek Granite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Biotite granite with subsidiary porphyritic microgranite.||||||
23190|Whitewater Creek Granite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province.|||||Grey to pink biotite granite with subsidiary porphyritic microgranite.|
24101|Whypalla Granite|24086|6|Mentioned|p312 Fig. 1|||||||||
24101|Whypalla Granite|24213|5|Briefly described|=|Permian|Permian|Of the Whypalla Supersuite.||||||01-JUN-09
24101|Whypalla Granite|42304|2|Defined|p22|Permian|Carboniferous|Reserved April 1988 by R.J. Bultitude||||||
24101|Whypalla Granite|42968|5|Briefly described|Fig. 1,p91,p99|||||||||
24101|Whypalla Granite|43625|6|Mentioned|p60|||||||||
24101|Whypalla Granite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Whypalla Supersuite. Geological Province: Kennedy Province.||||||02-JUN-09
24101|Whypalla Granite|60425|4|Described|p80, p274-5 Appdx. 1|Early Permian|Early Permian|Of Whypalla Suite (Whypalla Supersuite). S-type. Age: 278+/-4Ma (Rb-Sr). White, medium-coarse- grained, moderately to highly porphyritic muscovite-biotite granite; accessory garnet, zircon, apatite, monzonite?, ilmenite; detailed lithology included.||||||07-FEB-11
24101|Whypalla Granite|69592|5|Briefly described|p248, p249 Fig.4.34|Permian|Permian|Central Palmer-Barron Subprovince.||||Intrudes Hodgkinson Formation.||
24101|Whypalla Granite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Suite.||||
69322|Whypalla Suite|60425|5|Briefly described|p81 Tb. 5, p270 and p274-7 Appdx. 1|||Of the Whypalla Supersuite. Contains Whypalla Granite, Mount Windsor granite, Lang Creek and Koobaba Granites. S-type.||||||07-FEB-11
69322|Whypalla Suite|69593|5|Briefly described|p479|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Whypalla Supersuite.|Koobaba, Lang Creek, Whypalla, Mount Windsor Granites.|||
41258|Widbury Granite|50598|5|Briefly described|Map Legend|Early Triassic|Late Permian|Biotite granite to granodiorite.||||||
41258|Widbury Granite|61087|5|Briefly described|Map Legend|Late Permian|Late Permian|Grey, equigranular, fine to medium-grained, saccharoidal biotite granite to granodiorite with common microdiorite xenoliths and hornblende aggregates.||||||
41258|Widbury Granite|64398|5|Briefly described|Map legend|Early Permian|Early Permian|Grey, equigranular, fine- to medium-grained, saccharoidal biotite granite to granodiorite with common microdiorite xenoliths and hornblende aggregates.||||||14-AUG-08
41258|Widbury Granite|64399|5|Briefly described|Map legend|Early Permian|Early Permian|Grey, equigranular fine- to medium-grained saccharoidal biotite granite to granodiorite with common microdiorite xenoltihs and hornblende aggregates.||||||
41258|Widbury Granite|65388|3|Fully described|286-288, p285, 295, 41, 42, 265|Early Permian|Early Permian|New name. Of Coonambula Suite. Rocks previously included in Coonambula Granodiorite. Of Coonambula Suite. Has hornsfelsed the Nogo beds. Intruded by Boolgal Granophyre. SHRIMP U-Pb zircon age grouping: 290+/-5 Ma. Distinguished on basis of subtle variations in radiometric response. Isotopic and geochemical evidence suggests that the distinction between Widbury Granite and Coonambula Granodiorite may not be valid. May include McKonkey Granodiorite. Commonly comprises equigranular, saccharoidal fine-grained biotite granodiorite or granite. Also some grey hornblende-biotite granodiorite. See also p236, 296-297, 303, 304, 318, 340.||||||
41258|Widbury Granite|68679|5|Briefly described|p406, p408, p415|Permian|Permian|Auburn Subprovince, New England Orogen. May be part of the same unit with Coonambula Granodiorite. Strongly honfelsed the Nogo beds. Early Permian. Younger K-Ar age given.|290.4 +/- 4.9 Ma (SHRIMP U-Pb: Fanning et al.2009)|||?Intrudes the Nogo beds.|Equigranular, saccharoidal, fine-grained biotite granodiorite or granite; moderately to strongly foliated. Peraluminous, S-type.|
41258|Widbury Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|290+/-4.9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
41258|Widbury Granite|73450|6|Mentioned|p28|||Rawbelle Batholith.||||Intruded by Boolgal Granophyre.||
27305|Widdallion Sandstone Member|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Lawn Hill Formation.||||||07-NOV-08
27305|Widdallion Sandstone Member|23397|5|Briefly described|p476|||||||||
27305|Widdallion Sandstone Member|23964|5|Briefly described|p1269 Table 1|||Of Lawn Hill Formation. Geological Province: Mount Isa Inlier.||||||
27305|Widdallion Sandstone Member|24309|5|Briefly described|p1014|Proterozoic|Proterozoic|Of the Lawn Hill Formation.||||||19-DEC-06
27305|Widdallion Sandstone Member|37459|2|Defined|p433|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||19-DEC-06
27305|Widdallion Sandstone Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27305|Widdallion Sandstone Member|38310|6|Mentioned|p237|||||||||
27305|Widdallion Sandstone Member|38348|6|Mentioned|p22|||||||||
27305|Widdallion Sandstone Member|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Lawn Hill Formation.  Blocky to massive, thick-bedded, micaceous, cross-bedded medium quartz sandstone.||||||10-JAN-05
27305|Widdallion Sandstone Member|39497|4|Described|p14|||||||||
27305|Widdallion Sandstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27305|Widdallion Sandstone Member|39925|4|Described|p332|||||||||
27305|Widdallion Sandstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Lawn Hill Formation.||||||
27305|Widdallion Sandstone Member|45166|5|Briefly described|p30|||||||||
27305|Widdallion Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Lawn Hill Formation. Greyish red to brown, purple weathering, highly lithic and micaceous fine to coarse sandstone; minor glauconite; siltstone and claystone.||||||
27305|Widdallion Sandstone Member|65337|3|Fully described|p9 Fig.5, pp21-22, pp29-30.|Paleoproterozoic|Paleoproterozoic|50 - 370 m of inner shelf - high energy shoreface environment deposits. Forms low banded strike ridges.||Unit in Lawn Hill Formation.||Overlain disconformably, locally unconformably, by Playford Sandstone.|Greyish red to brown, purple-weathering, highly lithic and micaceous fine to coarse sandstone; minor glauconite; siltstone and claystone.|
27305|Widdallion Sandstone Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Isa Superbasin. Appears as Widdallion Sanstone[sic] in both Time-Space Plots.|1589 +/- 3 Ma.|Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|69433|4|Described|p18:2, 6, 10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 50-370m thick. A distinctive ridge-forming unit. Repeated progradational deposits in a high-energy shoreface environment.||Lawn Hill Formation.||Is overlain by South Nicholson Group disconformably or locally unconformably.|Lithic and micaceous, fine-, medium-, and less commonly coarse-grained sandstone; beds are medium to very thick, arranged in cycles from 5m to 20m thick which become coarser, better sorted, slightly less lithic, and lighter coloured upwards.|12-JUL-16
27305|Widdallion Sandstone Member|69434|6|Mentioned|p19:3|||Parent unit not named.||||Is overlain by Wangalinji Member disconformably (unconformably SW of Mitchiebo Waterhole).||12-JUL-16
27305|Widdallion Sandstone Member|69591|6|Mentioned|p43 Fig.2.31|||Isa Superbasin.||||||
27305|Widdallion Sandstone Member|69673|6|Mentioned|p52 fig 42, p54|||up to 370m thick.||McNamara Group|||Lithic and micaceous sandstone.|
27305|Widdallion Sandstone Member|71369|5|Briefly described|p9|||Lawn Hill Gorge area.||Lawn Hill Formation.||Is overlain unconformably by Hedleys Sandstone.||
27305|Widdallion Sandstone Member|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72527|3|Fully described|p1, p8, p12, p140-146, p193-195|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Unit varies in thickness from 50m to 370m. Sampled material is feldspathic sandstone.|1606+/-7 Ma max dep. age|Lawn Hill Formation?, McNamara Group||Overlies Lawn Hill Formation (presumably conformably) and unconformably underlies Wangalinji Member, Playford Formation.|Characterised by friable brown to purple lithic and micaceous fine to coarse-grained sandstone and minor laminated siltstone and claystone. Bedding is medium to very thick (several metres) with abundant pebble lags and gritty lenses.|
27305|Widdallion Sandstone Member|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Lawn Hill Formation, McNamara Group||Unconformably overlain by Wangalinji Member (Playford Sandstone, Wild Cow Subgroup, South Nicholson Group).||
27305|Widdallion Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Isa Superbasin.||||Underlain(?) by Lawn Hill Formation. Partly overlain by Hedleys Sandstone unconformably.||
27305|Widdallion Sandstone Member|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|Not shown what Formation this unit is a member of.||||||
27305|Widdallion Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|Isa Superbasin. Shown as included in both the Wide and Doom supersequences. Partial aquifer. Potential tight gas/oil.||Lawn Hill Formation, McNamara Group||||14-OCT-22
29600|Wide Bay Creek Gneiss|22845|6|Mentioned|p59-64,78||Late Carboniferous|Early marginal phase of the Claddagh Granodiorite.||||||
29600|Wide Bay Creek Gneiss|22846|6|Mentioned|p14|Carboniferous|Devonian|||||||
29600|Wide Bay Creek Gneiss|23251|6|Mentioned|p29|||Named by Don Chak & others (1995). Claddagh-Manumbar Assemblage.||||||
29600|Wide Bay Creek Gneiss|23799|6|Mentioned|p123|||Included in the "Claddagh-Manumbar Assemblage" of Little (1993).||||||
29600|Wide Bay Creek Gneiss|43588|6|Mentioned|p30||Late Devonian|||||||
29600|Wide Bay Creek Gneiss|44923|5|Briefly described|Map Legend||Carboniferous|||||||
29600|Wide Bay Creek Gneiss|50320|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
29600|Wide Bay Creek Gneiss|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones and Talamy Schist, are all mapped under the symbol, DCdm.||||||
29600|Wide Bay Creek Gneiss|68679|5|Briefly described|p322, p324-326, p331-332|Permian|Permian|Part of the Claddagh-Manumber Assemblage in the North D'Aguilar Subprovince. Occurs as narrow (<1km wide) belts S and E of Kilkivan. Synchronous with Manumbar Metamorphics and Claddagh Granodiorite and is interpreted as an early marginal phase of the latter, which it appears to underlie. Has two high-T metamorphic foliations.||||Is intruded by Karandah Granodiorite.|Thinly-laminated quartzofeldspathic gneiss, granoblastic and fine- to medium-grained.|
40576|Wide Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes upper parts of Balbirini Dolostone.|||
40576|Wide Supersequence|63866|6|Mentioned|p53|||Isa Superbasin.||||||
40576|Wide Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Calymmian|Statherian|Lawn Hill Platform.|1600-1585 Ma.|||Overlies Lawn Supersequence.|Shale, feldspathic sandstone.|
40576|Wide Supersequence|66843|5|Briefly described|p38-39|||Lawn Hill Platform. Depositional cycles and lithofacies detailed.||||||
40576|Wide Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40576|Wide Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Or Nathan Group, NT (p9). Camooweal - Murphy Domain, Mount Isa Inlier.||||Overlies Lawn Supersequence. Is overlain by Doom Supersequence.|Grey to black siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite|
40576|Wide Supersequence|68146|6|Mentioned|p4, p203|||Lawn Hill Platform and southern McArthur Basin.||||||
40576|Wide Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation.||||||
40576|Wide Supersequence|69591|5|Briefly described|p27, p43, p47, p54|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the middle part of Lawn Hill Formation. Generally coarsens upwards.||||Overlies Lawn Supersequence. Is overlain by Doom Supersequence. Is equated with upper part of Doomadgee Formation.||
40576|Wide Supersequence|70897|5|Briefly described|p39,40,  Fig.1.7.2-3,7|Mesoproterozoic|Mesoproterozoic|Shows rapid thickness and lithofacies variations across regional fault systems. Age from underlying Lawn Hill Formation tuff.|Max age 1595 +/- 6 Ma (Page and Sweet, 1998).|||||22-SEP-18
40576|Wide Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Widdallion Sandstone Member.|||||Grey to brown, siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite.|
40576|Wide Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||||
40576|Wide Supersequence|72912|5|Briefly described|p17, p33 Fig.12, p34, p35 Fig.13.|||||||||15-MAR-21
40576|Wide Supersequence|73144|4|Described|p8-9, p12-13, p20, p25|Calymmian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains three third order sequences [see article for more detail on third order sequences]. Deposited via outer shelf turbidites or silty prograding lowstand wedge (Krassay et al., 2000). Oldest measured age 1595 +/- 6 Ma [no further age detail]. Upward coarsening. Lower portion is characterized by dolomitic limestone and siltstone, while the upper portion comprise arkosic sandstone and siltstone. Contemporaneous deposition with the Wide Event, at ~1595 Ma associated with west to north-west transtension.|1585-1600 Ma|||Includes a portion of the Lawn Hill Formation.|Silty shale, dolostone, dark grey carbonaceous siltstone and sandy siltstone, siltstone and lithic sandstone.|
29601|Widgee Metamorphics|22845|2|Defined|p12,14,21-5,32,77,80|Early Carboniferous|Late Devonian|Interlayered with Gogongo Metamorphics.  Correlates with Wongella Metamorphics.||||||
29601|Widgee Metamorphics|22846|6|Mentioned|p58|Carboniferous|Devonian|Intruded by Station Creek Quartz Monzonite.||||||
29601|Widgee Metamorphics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
29601|Widgee Metamorphics|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
29601|Widgee Metamorphics|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
29601|Widgee Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
29601|Widgee Metamorphics|68679|5|Briefly described|p325-329|||Little (1993). Kilkivan-Manumbar area, North D'Aguilar Subprovince. Mapped as large slabs (up to 2 km2) or as smaller inclusions (to pebble size) in Mount Mia Serpentinite. Lower plate accretionary assemblage. RELATED UNITS (continued): Equivalent to Rocksberg and Peters Creek Greenstones and Wongella Metamorphics.||||Intruded by Rush Creek Granodiorite. Interlayered locally with Gobongo Metamorphics. Structurally underlies Mount Mia Serpentinite. Is faulted under and against Amamoor beds. See COMMENTS for more.|Massive to schistose, mafic tremolite-actinolite-chlorite schist, serpentinite, greenschist. Protolith was metadolerite to metagabbro.|
30703|Widgewarra Granite|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30703|Widgewarra Granite|50536|5|Briefly described|p1.5, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Sybella Suite.||||||07-NOV-08
30703|Widgewarra Granite|63023|6|Mentioned|p1035 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Sybella Suite. Age: 1670+/-3Ma (SHRIMP U-Pb). ||||||07-NOV-08
30703|Widgewarra Granite|64744|6|Mentioned|p357 Table 1. |Statherian|Statherian|Southern Sybella region. Mylonitic with lineation.|1670 +/- 3 Ma.|||||
30703|Widgewarra Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Sybella Domain, Mount Isa Inlier. Sybella Igneous Event. Exhibits NW trending linear fabric (Widgeewarra pluton p12).|1670 +/- 3 Ma.|Sybella Suite.|||Foliated coarse porphyritic biotite granite.|
30703|Widgewarra Granite|69591|5|Briefly described|p59|||Sybella Batholith.|1670 +/- 3 Ma (Neumann et al., 2006).||||Foliated coarse porphyritic biotite granite.|
30703|Widgewarra Granite|71592|5|Briefly described|Appendix A.|||Sybella Domain, Mount Isa Orogen.|1670+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
80558|Wigan Granite|71792|2|Defined|p10, p30, p33, p49-p54|Early Permian|Early Permian|Coen Inlier. Previously defined as Wigan Adamellite. This unit is named for the Parish of Wigan. The type area is the hills north and south of the Wenlock River junction with Sefton Creek, around 13.1333'S 143.0333'E. Exposed to the east of the Mesozoic sandstone cover in the northern part of the Coen 1:250k sheet area. Initially defined by Whitaker & Willmott (1969) as the Wigan Adamellite. The unit was assigned a devonian age by Whitaker & Gibson, 1977), Cooper et al (1975) subsequently reported a Rb-Sr age of 283 Ma. Referred to as the Wigan Adamellite on p10. Intrudes unit Dgk/9. This zoned pluton includes a highly magnetic core which is mapped as subunit 1 and described seperately in this volume. This subunit 1 was previously mapped as Flyspeck Granodiorite but has now been included in the Wigan Granite on the basis of geophysical evidence. Distribution, geophysical characteristics and outcrops characteristics are discussed. A Rb-Sr whole rock age of 281-283 Ma is derived from Webb (1969) and recalculated by Day et al, 1983 to 277 +/- 2 Ma. Magnetic data suggests this unit intrudes the Weymouth Granite.|277 +/- 2  Ma (Rb-Sr whole rock)|Weymouth Supersuite||Intrudes Weymouth Granite. Intrudes the Yarraden Schist. Faulted against the Wolverton Granite.|Leucocratic biotite monzogranite and syenogranite, tonalite, medium-grained equigranular hornblende granodiorite, coarse- to medium-grained, porphyritic biotite-garnet granite. Pegmatite and aplite occur towards the margins of this unit.|10-AUG-18
80558|Wigan Granite|71853|5|Briefly described|Map legend.|Permian|Permian|The two facies are mapped separately.|||||Leucocratic biotite monzogranite and syenogranite, biotite monzogranite and granodiorite. Grey, medium-grained equigranular to mildly porphyritic hornblende-biotite granite.|
80558|Wigan Granite|71854|5|Briefly described|Map legend.|Permian|Permian|The two facies are mapped separately.|||||Leucocratic biotite monzogranite and syenogranite, biotite monzogranite and granodiorite. Grey, medium-grained, equigranular to mildly porphyritic hornblende-biotite granite.|
80558|Wigan Granite|72983|6|Mentioned|p56|||||||Intrudes Coen Metamorphic Group including[?] Yarraden Schist.|Hornblende- and biotite-bearing I-type granite.|
76890|Wiggle Waterhole Metagabbro|67323|5|Briefly described|GIS attrib tbl; p20|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event. Forms small, very widespread intrusions in the southen half of the Doherty-Fig Tree Gully Domain.||Williams Supersuite.|||Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro|
76890|Wiggle Waterhole Metagabbro|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro|
76890|Wiggle Waterhole Metagabbro|70353|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|70354|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|70355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|70356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||||Mainly small intrusions into Staveley Formation.|Hornblende diorite and metagabbro.|05-MAY-16
76890|Wiggle Waterhole Metagabbro|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Doherty-Fig Tree Gully Domain.||||Intrudes Staveley Formation.||
76890|Wiggle Waterhole Metagabbro|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Doherty-Fig Tree Gully Domain.||||Intrudes Staveley Formation.|Hornblende diorite and metagabbro.|20-JAN-22
76890|Wiggle Waterhole Metagabbro|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Doherty-Fig Tree Gully Domain.||||Intrudes Staveley Formation.|Hornblende diorite and metagabbro.
|
76890|Wiggle Waterhole Metagabbro|72682|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Age uncertain. Shown as Paleoproterozoic, possibly ranging into the Mesoproterozoic. Potentially associated with Isan Orogeny (1590-1500Ma). Part of the Marimo-Staveley Domain.||||Possibly coeval with Florence Creek Granite.|Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|72683|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Age uncertain. Shown as Paleoproterozoic, possibly ranging into the Mesoproterozoic. Potentially associated with Isan Orogeny (1590-1500Ma). Part of the Marimo-Staveley Domain.||||Possibly coeval with Florence Creek Granite.|Hornblende diorite and metagabbro.|
76890|Wiggle Waterhole Metagabbro|72889|6|Mentioned|p8.|||||||||
36252|Wilderness Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
36252|Wilderness Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
36252|Wilderness Granite|60425|4|Described|p285 Appdx., p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Included in Black Prince Granite., together with Brownville, Disaster, Glenlinedale and Stingo Granites on most recent maps. Fine-grained, granophyric biotite granite. I-type.||||||07-FEB-11
34210|Wiley Igneous Complex|22515|6|Mentioned|p402||Calymmian|Informal name for pluton of Saxby Granite? Max Age: U-Pb zircon of 1520 Ma.||||||
34210|Wiley Igneous Complex|22667|6|Mentioned|P243|||||||||
34210|Wiley Igneous Complex|23967|4|Described|p1332|Mesoproterozoic|Mesoproterozoic|||||||
34210|Wiley Igneous Complex|24257|5|Briefly described|p72 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological Province: Eastern fold belt, Mount Isa Block.||||||
34210|Wiley Igneous Complex|60665|6|Mentioned|p1157 Fig.9, |Calymmian|Calymmian|Southern Cloncurry intrusion. Age inferred from Fig.9.|1520 +/- 8 Ma.|||||
34210|Wiley Igneous Complex|65396|5|Briefly described|p57, p363-364, p377|||Mis-spelt as Whiley Igneous Complex on p363.  >23 km2 N-S elongate ovoid-shaped composite pluton on E side of the Cloncurry Fault. Is said to represent the southern-most mass of the Saxby Granite. The diagram on p364 shows constituent units with [presumably informal] names: Block, Roadrunner, Coyote Granites and Emu Dolerite.||Cloncurry Supersuite.|||Includes leucogranite, mafic igneous rocks, biotite-hornblende intrusions, hybrid igneous rocks.|
33426|Wilfred Creek Igneous Complex|23799|3|Fully described|p84, p11 Tb. 1|Late Triassic|Middle Triassic|Mixed intrusions of dark grey, medium-grained hornblende (biotite) diorite, quartz diorite, tonalite and rare gabbro; local monzogranite.  of the South-east Queensland Volcanic and Plutonic Intrusives.||||||
33426|Wilfred Creek Igneous Complex|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
33426|Wilfred Creek Igneous Complex|64398|5|Briefly described|Map legend|Early Triassic|Late Permian|Mixed intrusions of dark ghrey, medium-grained, hornblende(-biotite) diorite, quartz diorite, tonalite and rare gabbro; local monzogranite.||||||
33426|Wilfred Creek Igneous Complex|68679|5|Briefly described|p414-415|Middle Triassic|Late Permian|West of the Esk Basin, northern New England Orogen. Two bodies north of the Boondooma Igneous Complex. Higher in alkalis and relatively depleted in CaO.|245 +/- 7 Ma (K-Ar: Whitaker et al., 1974).||||Diorite, quartz diorite, tonalite and rare gabbro; zone of monzogranite with abundant mafic xenoliths.|08-DEC-21
33426|Wilfred Creek Igneous Complex|73450|6|Mentioned|p36|||||||Intruded by Toondahra Granite.||
36459|Wilkie Gray Group|23422|4|Described|p180, p206 Table 6.3|Middle Devonian|Early Devonian|||||||
36459|Wilkie Gray Group|23430|5|Briefly described|p505|||Consists of Mount Podge Limestone and Laroona Formation.||||||
36459|Wilkie Gray Group|23509|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|||||||
36459|Wilkie Gray Group|23522|5|Briefly described|p258|Middle Devonian|Early Devonian|||||||
36459|Wilkie Gray Group|23893|5|Briefly described|p15|Eifelian|Emsian|Geological Province: Broken River Province.||||||
36459|Wilkie Gray Group|24577|5|Briefly described|p752 Fig. 1|Emsian|Pragian|Unconformably overlies the Argentine and Running River Metamorphics. Group is Gp in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||20-JUN-13
36459|Wilkie Gray Group|24614|4|Described|p191 Fig. 1, p192|Emsian|Emsian|Units of this group (Laroona Arkose + Mount Podge Limestone) were formerly incorporated into the Fanning River Group - now excised + assigned to Fanning River Group (Talent + Mawson 1994). Geological Province: Burdekin Basin. See also p193 Fig. 2.||||||07-FEB-11
36459|Wilkie Gray Group|68350|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.|||Includes Laroona Formation and Mount Podge Limestone.|||
36459|Wilkie Gray Group|68351|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Burdekin Basin.|||Includes Laroona Formation and Mount Podge Limestone.|||
36459|Wilkie Gray Group|68419|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Burdekin Basin.|||Includes Mount Podge Limestone.|||
36459|Wilkie Gray Group|68420|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Of the Burdekin Basin.|||Includes Mount Podge Limestone.|||
36459|Wilkie Gray Group|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Burdekin Basin.||||||
36459|Wilkie Gray Group|68731|5|Briefly described|p183, 184 Fig 3.98, p185 Tb 3.4|Early Devonian|Early Devonian|Draper and Land (1994). Burdekin Basin. A basinal outlier near the boundary of the Charters Towers Province is tentatively assigned to this Group. Assigned Group status by Zhen, Lang, and Jell (1993).|||Includes the Mount Podge Limestone and the Laroona Formation.||Comprises predominantly shallow-marine carbonates.|18-JUL-14
36459|Wilkie Gray Group|68900|6|Mentioned|p32|Early Devonian|Early Devonian|Townsville area. Underlies the Burdekin Basin.||||||
36459|Wilkie Gray Group|70740|6|Mentioned|p36|||||||||
36524|William Creek complex|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 177.||||||
30680|Williams Supersuite|23545|5|Briefly described|p605|||||||||
30680|Williams Supersuite|24197|5|Briefly described|p7, p31, p92|Proterozoic|Proterozoic|Comprises major part of Williams and Naraku Batholiths. Extremely heterogeneous, consisting of series of compositionally distinct (granodioritic) type intrusions. Age: 1560-1480Ma. Geol.Prov: Mount Isa Inlier. Example of Hiltaba Assoc.||||||07-FEB-11
30680|Williams Supersuite|50100|5|Briefly described|p21, p61|Proterozoic|Proterozoic|Of the Williams Batholith.  Includes the Williams, Saxby, Mount Dore, Wimberu, Yellow Waterhole, Mount Angelay, Mount Cobalt and Squirrel Hills  Granites.  ||||||
30680|Williams Supersuite|50332|5|Briefly described|p22|Mesoproterozoic|Mesoproterozoic|Includes; Naraku + Williams Batholiths, Naraku Granite, Capsize Granodiorite, Malakoff Granite, Williams Granite and Mount Margaret Granite. Geol Prov: Quamby-Malbon and Cloncurry Subprovinces. Dominantly felsic rocks.||||||07-FEB-11
30680|Williams Supersuite|50536|5|Briefly described|p1.1, 10.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Age: 1510Ma. See also Williams Suite.||||||
30680|Williams Supersuite|63776|6|Mentioned|p1089, p1100|||Age: 1500-1350 Ma. Geological Province: Mt Isa Inlier.||||||02-JUN-16
30680|Williams Supersuite|65396|6|Mentioned|p301|||Includes Williams and Naraku Batholiths. Considered by Budd et al. (2002) to have the best metallogenic potential in the Mount Isa Inlier.||||||
30680|Williams Supersuite|65455|6|Mentioned|p7, p8 Fig. 4|Mesoproterozoic|Mesoproterozoic|Eastern Fold Belt, Mount Isa Region. Shows overall elevated U contents, the most concentrated occurrences of U-enriched igneous rocks in the Mount Isa Region.||||||
30680|Williams Supersuite|66529|5|Briefly described|p60, p77 |Mesoproterozoic|Mesoproterozoic|Elevated concentrations of U; possible primary U source for local sandstone-hosted systems. Contains moderate to highly prospective granitoids for orthomagmatic U deposits. Has highest Hot Rock heat production values. Also appears as Naruku-Williams Granite Suite on p5; Williams Suite on p16; on p45 as Williams-Naruku Granites and Williams-Naruku granite suite; as Williams-Naraku suite on p53.|Between 1530 and 1500 Ma.|||||
30680|Williams Supersuite|67323|4|Described|p15, p17, p19-21, p28, p37, p45, p107|Mesoproterozoic|Mesoproterozoic|See also GIS attrib tbl, Solid Geology Map. Williams Igneous Event: synchronous with Late Isan Orogeny; associated with extensive potassic alteration and IOCG mineralisation. Forms a N-S trending belt in the eastern parts of the Mount Isa Inlier; interpreted as having formed over a hotspot. Generally variably magnetic and with low gravity responses. Appears as William Supersuite on p15; included in a list of Suites on p41. CONSTITUENTS (continued): Black Eye, Florence Creek, Kays Peak, Lowman Tank, Malakoff, Mount Angelay, Mount Cobalt, Mount Dore, Mount Margaret, Myla, Naraku, Nundata, Repeater Station, Saxby, Squirrel Hills, Wimberu, Yellow Waterhole Granites.|c.1550-1500 Ma.||Boorama Tank, Oorindimindi Gneisses; Dipvale, Mavis Granodiorites; Cowie Suite, Dingo Prospect Skarn, Foxes Creek Diorite, Mallee Gap Tonalite, Wiggle Waterhole Metagabbro. See COMMENTS for granites.|Intrudes Roxmere Quartzite, Staveley Formation, Soldiers Cap Group and Kuridala Group.|Extensive emplacement of A- and I-type granitic batholiths. Porphyritic biotite- and biotite-hornblende granite, granodiorite and minor diorite.|
30680|Williams Supersuite|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Mount Isa Province.||||||
30680|Williams Supersuite|68576|6|Mentioned|Q_2: p1|Mesoproterozoic|Mesoproterozoic|Mount Isa area.||||||
30680|Williams Supersuite|69056|5|Briefly described|p2,p4-6,p56-57, Reference images sheet.|||Shown on the simplified surface and solid geology maps of the Quamby Project area. Includes Williams, Naraku and Wimberu batholiths. Unnamed undercover intrusions have been defined on the basis of their magnetic responses: low-moderate in Constantine Domain, moderate-high in the Soldiers Cap Domain. Mafic phases have been linked to IOCG mineralisation.|~1540-1500 Ma.||Malakoff, Mount Margaret Granites; Mavis Granodiorite.||Potassium-rich, A-type granitoids and mafic rocks. The granites underwent fractionation and localised magma mixing and mingling.|
30680|Williams Supersuite|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||Yellow Waterhole Granite, Squirrel Hills Granite, Wimberu Granite, Wiggle Waterhole Metagabbro|||
30680|Williams Supersuite|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic||||Yellow Waterhole Granite, Squirrel Hills Granite, Wimberu Granite, Wiggle Waterhole Metagabbro|||
30680|Williams Supersuite|69582|4|Described|p20-p22, p24-p26, p28-p29|Mesoproterozoic|Mesoproterozoic|Millungera Basin. Targeted for geothermal energy potential. Intersected in GSQ Dobbyn 2 and GSQ Julia Creek 1 with heat flows of 107.5 +/- 1.7 mW/m^2 and 113 +/- 2.9 mW/m^2 respectively. Includes the Williams and Naraku plutons. Average density is modelled at 2.67 g/cm^3. Equivalent to intrusives in the Carpentaria Basin.||||Intrudes the Soldiers Cap Group.|I and A-type granitic rocks enriched in U, Th and K.|
30680|Williams Supersuite|69591|4|Described|p28, p41, p51, p59|Mesoproterozoic|Mesoproterozoic|Forms the Williams, Naraku and Wimberu batholiths. Units underwent fractionation, localised magma mixing and mingling. They show elevated LILE and HFSE concentrations, and enrichment in Co and Sr. The lithologies and ages of plutons in the Supersuite are tabulated on p59. CONSTITUENTS (continued): Monakoff, Mount Angelay, Saxby, Squirrel Hills, Yellow Waterhole, Florence Creek, Hamilton River, Kays Peak, Lowman Tank, Malakoff, Mount Cobalt, Mount Dore, Mount Margaret, Myla, Naraku, Nundata and Wimberu Granites.|~1540-1500 Ma.|Squirrel Hills Granite.|Capsize Creek, Mavis Granodiorite; Foxes Creek Diorite; Mallee Gap Tonalite. For the numerous granites, see COMMENTS.||A-type granitoids.|
30680|Williams Supersuite|70353|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||Repeater Station, Nundata, Malakoff Granites.||Granite; porphyritic biotite and biotite-hornblende granite, granodiorite and minor diorite; minor hornblende gabbro to tonalite.|
30680|Williams Supersuite|70354|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic||||Repeater Station, Nundata, Malakoff Granites.||Granite; porphyritic biotite and biotite-hornblende granite, granodiorite and minor diorite; minor hornblende gabbro to tonalite.|
30680|Williams Supersuite|70355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Malakoff Granite.||Granite, granodiorite, monzodiorite.|
30680|Williams Supersuite|70356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Malakoff Granite.||Granite, granodiorite, monzodiorite.|
30680|Williams Supersuite|70532|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||Mavis Granodiorite, Malakoff Granite.||Granite, granodiorite.|
30680|Williams Supersuite|70570|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Associated with the 1590-1500 Ma Isan Orogeny.|||Squirrel Hills Suite, Saxby Granite, Myla Granite, Mount Angelay Granite, Kays Peak Granite, Nundata Granite, Mallee Gap Tonalite, Oorindimindi Gneiss, Lowman Tank Granite, Foxes Creek Diorite.|||05-MAY-16
30680|Williams Supersuite|70571|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic||||Includes Squirrel Hills Suite, Saxby, Myla Granites, Mount Angelay Granite, Kays Peak Granite, Nundata Granite, Mallee Gap Tonalite, Oorindimindi Gneiss, Lowman Tank Granite, Foxes Creek Diorite.|||
30680|Williams Supersuite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes two unnamed subsurface units: foliated leucocratic tonalite and pegmatite; porphyritic biotite and biotite-hornblende granite.|||Includes Hamilton River Granite, Yellow Waterhole Granite, Mount Dore Granite, Mount Cobalt Granite, Squirrel Hills Suite, Mallee Gap Tonalite, Lowman Tank Granite.|||20-JAN-22
30680|Williams Supersuite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes two unnamed subsurface units: foliated leucocratic tonalite and pegmatite; porphyritic biotite and biotite-hornblende granite.|||Includes Lowman Tank Granite, Mallee Gap Tonalite, Squirrel Hills Suite, Mount Cobalt Granite, Mount Dore Granite, Yellow Waterhole Granite, Hamilton River Granite.|||
30680|Williams Supersuite|70574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes an unnamed member of porphyritic biotite and biotite-hornblende granite, granodiorite and minor diorite.|||Includes Malakoff Granite, Mavis Granodiorite and one unnamed subsurface member.|||
30680|Williams Supersuite|71382|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|Intrudes the Eastern Fold Belt of the Mount Isa Inlier, outcropping over 2400km^2 to the west of the basin. Dominated by the Williams and Naraku batholiths which were emplaced after the Isan Orogeny D2 event. Interpreted to be derived from a source in the lower crust. Heat production detailed.||||Intrudes the Soldiers Cap Group.|Dominantly I-type granitic rocks enriched in U, Th and K.|
30680|Williams Supersuite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1512+/-5 Ma (U-Pb zircon SHRIMP)||||Granite.|
30680|Williams Supersuite|71799|6|Mentioned|p151 fig 3, p152|||Mount Isa Region.||||||
30680|Williams Supersuite|72596|6|Mentioned|p4|||Distribution shown in Fig i.||||||
30680|Williams Supersuite|72682|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Occurs across Mitakoodi, Marimo-Staveley and Doherty-Fig Tree Gully Domain areas. Associated with Isan Orogeny (1590-1500 Ma).|||Includes Squirrel Hills Granite, Florence Creek Granite and Wimberu Granite.||Porphyritic biotite and biotite-hornblende granite, granodiorite and minor diorite.|30-JUL-20
30680|Williams Supersuite|72683|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Occurs across Mitakoodi, Marimo-Staveley and Doherty-Fig Tree Gully Domain areas. Associated with Isan Orogeny (1590-1500 Ma).|||Includes Squirrels Hills Granite, Florence Creek Granite and Wimberu Granite.|||
30680|Williams Supersuite|72799|6|Mentioned|p4|||||||||
30680|Williams Supersuite|72889|6|Mentioned|p6 Fig.i, p28||||c.1550-1500 Ma.|||||
30680|Williams Supersuite|73137|6|Mentioned|p6, p81|Mesoproterozoic|Mesoproterozoic||||||Includes granite[?].|
30680|Williams Supersuite|73429|6|Mentioned|p114-115|Calymmian|Calymmian|Mount Isa Inlier. Predominantly A-type magmatism.|c. 1540-1500 Ma|||||
30680|Williams Supersuite|73525|6|Mentioned|p3|Calymmian|Calymmian|Voluminous A-type granitoids.|ca. 1540-1490 Ma|||||
30680|Williams Supersuite|73529|6|Mentioned|p15 Fig.11|Calymmian|Calymmian||1540-1500 Ma|||||
30680|Williams Supersuite|73553|5|Briefly described|p4-5, p44, p118, p165,|Calymmian|Calymmian|Williams-Naraku Igneous Province. See also p200, p210, p221, p266.|1540-1500 Ma||Mavis Granodiorite, Wimberu Granite|||03-FEB-23
36566|Willie Moore Creek rhyolite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 239.  I-Type.||||||
27935|Wimberu Granite|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Leached and silicified granite.||||||
27935|Wimberu Granite|22461|6|Mentioned|Fig 1 p464.|||||||||
27935|Wimberu Granite|22465|6|Mentioned|p934|||||||||
27935|Wimberu Granite|22515|3|Fully described|Fig1p398,402-4,406-8|Calymmian|Calymmian|U-Pb zircon age of 1508 (+/-) 4 Ma (Page 1993); Rb-Sr age of 1498 Ma (Richards 1966).||||||
27935|Wimberu Granite|22522|6|Mentioned|p332|||||||||
27935|Wimberu Granite|22667|5|Briefly described|Fig1 P234, P241||Calymmian|Age of unit is 1508+/-4 Ma||||||
27935|Wimberu Granite|23471|5|Briefly described|p110 Fig 1|Calymmian|Calymmian|Age: 1516-1508 Ma (U-Pb SHRIMP). Geological Province: Mount Isa Block.||||||
27935|Wimberu Granite|23519|5|Briefly described|p128|Mesoproterozoic|Mesoproterozoic|See also p106 Fig 1. Age: ~1508 Ma. Geological Province: Williams Batholith.||||||
27935|Wimberu Granite|23545|5|Briefly described|p606 Table 1.|||||||||
27935|Wimberu Granite|23967|6|Mentioned|p1331|||||||||
27935|Wimberu Granite|24039|6|Mentioned|p457 Fig.2|||||||||
27935|Wimberu Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
27935|Wimberu Granite|24254|6|Mentioned|p17 Fig.1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
27935|Wimberu Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Geological Province: Mount Isa Block. Age: ~1512-1504Ma (U-Pb)||||||
27935|Wimberu Granite|24257|5|Briefly described|p72 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological Province: Eastern fold belt, Mount Isa Block.||||||
27935|Wimberu Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
27935|Wimberu Granite|24462|5|Briefly described|p296 Fig. 1|||Geological Province: Mount Isa Block.||||||
27935|Wimberu Granite|29965|6|Mentioned|p402|||||||||
27935|Wimberu Granite|30530|6|Mentioned|p515|||Also mention P516.||||||
27935|Wimberu Granite|30531|6|Mentioned|p20|||See also mention Fig.2||||||
27935|Wimberu Granite|30725|6|Mentioned|p579|||||||||
27935|Wimberu Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27935|Wimberu Granite|32660|5|Briefly described|Table 5|||||||||
27935|Wimberu Granite|32959|6|Mentioned|Fig.21|||||||||
27935|Wimberu Granite|33900|6|Mentioned|p15|||||||||
27935|Wimberu Granite|35074|6|Mentioned|Fig.2|||||||||
27935|Wimberu Granite|35139|6|Mentioned|p10|||||||||
27935|Wimberu Granite|37462|4|Described|Table4.VII|||||||||
27935|Wimberu Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27935|Wimberu Granite|37862|6|Mentioned|p587|||||||||
27935|Wimberu Granite|38350|4|Described|p20|||||||||
27935|Wimberu Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27935|Wimberu Granite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27935|Wimberu Granite|39445|6|Mentioned|p43|||See also Table 2||||||
27935|Wimberu Granite|39496|4|Described|p15|||||||||
27935|Wimberu Granite|40840|6|Mentioned|Map legend|||||||||
27935|Wimberu Granite|41791|6|Mentioned|p250|||||||||
27935|Wimberu Granite|41979|5|Briefly described|p532|||||||||
27935|Wimberu Granite|43490|6|Mentioned|8|||U-Pb Zircon Age: 1508+/-4Ma||||||
27935|Wimberu Granite|44091|14|Not recorded|p10||Paleoproterozoic|||||||07-NOV-08
27935|Wimberu Granite|44195|5|Briefly described|p345 Table 1,355|||Informal name. U-Pb age 1508+/-4 Ma. See also p358.||||||
27935|Wimberu Granite|44257|14|Not recorded|p19,21|||Rb-Sr. 1540 Ma. May be material of deep seated origin.||||||
27935|Wimberu Granite|44271|2|Defined|p37,38,46|||||||||
27935|Wimberu Granite|44275|14|Not recorded|Map Legend|||||||||
27935|Wimberu Granite|44276|4|Described|p11,12,map|||||||||
27935|Wimberu Granite|44749|14|Not recorded|p25|||||||||
27935|Wimberu Granite|44751|14|Not recorded|p300||Precambrian|||||||
27935|Wimberu Granite|44806|14|Not recorded|p282|||Petrographic description.||||||
27935|Wimberu Granite|44849|14|Not recorded|p69,74,75,82,93|||||||||
27935|Wimberu Granite|44989|2|Defined|p.147-8|||Tb.IV,VI. (F54-6). On many pages.||||||
27935|Wimberu Granite|45003|14|Not recorded|p21|||||||||
27935|Wimberu Granite|45087|5|Briefly described|p29|||Chemical analyses||||||
27935|Wimberu Granite|45161|4|Described|p51|||||||||
27935|Wimberu Granite|45166|5|Briefly described|p61|||||||||
27935|Wimberu Granite|45287|14|Not recorded|p.230|||||||||
27935|Wimberu Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
27935|Wimberu Granite|48894|6|Mentioned|p31|||1432my. See P47.||||||
27935|Wimberu Granite|48906|14|Not recorded|p4,25,27|||||||||
27935|Wimberu Granite|49041|5|Briefly described|Table 3|||Mention Table 4||||||
27935|Wimberu Granite|50100|5|Briefly described|p13 Fig. 4, p21|Calymmian|Calymmian|Of the Williams Supersuite.  Age: ~1500Ma.  Geological Province: Eastern Fold Belt.||||||
27935|Wimberu Granite|50536|5|Briefly described|p1.5, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite/Supersuite. Age: 1508 +/- 4Ma (Shrimp).||||||
27935|Wimberu Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
27935|Wimberu Granite|60665|6|Mentioned|p1157 Fig.9. |Calymmian|Calymmian|Southern Cloncurry intrusion. Age inferred from Fig.9.|1508 +/- 4 Ma.|||||
27935|Wimberu Granite|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. See also p59 Fig. 4.||||||
27935|Wimberu Granite|61926|5|Briefly described|p71 Fig. 1|||Part of the Williams Batholith. Geological Province: Eastern Fold Belt, Mount Isa Inlier. See also p73 Fig. 3. ||||||
27935|Wimberu Granite|61933|5|Briefly described|p169 Fig.3|Mesoproterozoic|Mesoproterozoic|Pluton of the Williams and Naraku Batholiths. Age: 1516-1490 Ma.||||||
27935|Wimberu Granite|61936|5|Briefly described|p200|||A-type, metaluminous, magnetite-bearing plutonic rocks of the Isan Orogeny. ||||||
27935|Wimberu Granite|62047|6|Mentioned|p90 Fig.1 |||||||||
27935|Wimberu Granite|63866|5|Briefly described|p62|Calymmian|Calymmian|Intrudes stratigraphic units of the Mitakoodi Anticline and Marimo-Stavely Zone. Numeric age is interpreted as the age of magmatic crystallisation.|1509 +/- 4 Ma (Page and Sun, 1998)|||||
27935|Wimberu Granite|64248|6|Mentioned|p33 Fig.1, p45|||A composite intrusion, containing several discrete intrusions that may have approximately internal concentric zones and a wide range of compositions.||||||
27935|Wimberu Granite|64250|6|Mentioned|Figs.1-3, 5; p15||||1512 +/-4 Ma; 1508 +/-4 Ma.|||||
27935|Wimberu Granite|65396|5|Briefly described|p4, p7, p21-22, p40, p53, p56, p61, p82|Calymmian|Calymmian|See also p104, p157, p172-173, p175, p179, p213, p223-224, p241, p272, p276, p327, p360-361, p438, p440, p445, p474-500. Mount Isa Inlier. Associated with the Isan Orogeny. Composite body: several discrete intrusions. Appears as Wimberu granite on p223 and p276. Stress partitioning and fluid flow models detailed.|1508 +/- 4 Ma (SHRIMP: Page and Sun, 1998)|||||04-APR-17
27935|Wimberu Granite|66913|5|Briefly described|p170 fig 1, p171 fig 2, p174, 188|Calymmian|Calymmian|U-Pb zircon SHRIMP age shown diagramatically on Fig. 2. Age discussed p188 as likely being hydrothermal alteration age.|1476 +/- 4 Ma from breccias. |||||
27935|Wimberu Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p16, p72. Mitakoodi and Marimo-Staveley Domains, Mount Isa Inlier. Williams Igneous Event. Low gravity response. Contains a Zn anomaly.|1508 +/- 4 Ma and 1512 +/- 4 Ma.|Williams Supersuite.|||Porphyritic and non-porphyritic biotite, hornblende, and hornblende-biotite granite and granodiorite; minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite|
27935|Wimberu Granite|68542|6|Mentioned|p18|||||||||
27935|Wimberu Granite|68576|6|Mentioned|Q_2: p16, p18|||An intrusive phase of the 1545-1500 Ma Williams/Naraku Batholith, S of Cloncurry.||||||
27935|Wimberu Granite|68732|6|Mentioned|p158 Fig.1|||||||||
27935|Wimberu Granite|69056|6|Mentioned|Time-Space plot sheet|Calymmian|Calymmian||1512 +/- 4 Ma; 1508 +/- 4 Ma.|||||
27935|Wimberu Granite|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Porphyritic and non-porphyritic biotite, hornblende, and hornblende-biotite granite and granodiorite; minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite (subsurface)|
27935|Wimberu Granite|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Porphyritic and non-porphyritic biotite, hornblende, and hornblende-biotite granite and granodiorite; minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite|
27935|Wimberu Granite|69549|6|Mentioned|p95|Calymmian|Calymmian|Shown as Wimberu granite.|1508 +/- 4 Ma.|||||16-NOV-16
27935|Wimberu Granite|69591|5|Briefly described|p51, p59|||Eastern Mount Isa Province; late Isan Orogeny.|1508 +/- 4 Ma (Page and Sun, 1998).|Williams Supersuite.|||A-type granitoid.|
27935|Wimberu Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1508+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
27935|Wimberu Granite|72682|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Mitakoodi Domain area. Includes 3 informal lithological divisions within unit.||Williams Supersuite||Probably coeval with Florence Creek Granite. Intrudes Mitakoodi Quartzite (indicated by roof pendants).|Includes porphyritic and non-porphyritic biotite, hornblende and hornblende-biotite granite and granodiorite, minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite|
27935|Wimberu Granite|72683|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Within the Mitakoodi Domain area. Includes 3 informal lithological divisions within unit.||Williams Supersuite||Probably coeval with Florence Creek Granite. Intrudes Mitakoodi Quartzite (indicated by roof pendants).|Includes porphyritic and non-porphyritic biotite, hornblende and hornblende-biotite granite and granodiorite, minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite.|
27935|Wimberu Granite|72684|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Intrudes part of the Mitakoodi Domain, coeval with the Isan Orogeny (1590-1500 Ma).||||Shown as coeval with Florence Creek Granite.|Porphyritic and equigranular biotite, hornblende, and hornblende-biotite granite and granodiorite; minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite.|
27935|Wimberu Granite|72685|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Intrudes part of the Mitakoodi Domain, coeval with the Isan Orogeny (1590-1500 Ma).||||Shown as coeval with Florence Creek Granite.|Porphyritic and equigranular biotite, hornblende, and hornblende-biotite granite and granodiorite; minor leucogranite, pyroxene-bearing granite, microgranite, aplite, pegmatite.|
27935|Wimberu Granite|72799|4|Described|p1-3, p12-16, p32|Calymmian|Calymmian|Williams/Naraku Batholiths. Forms a large composite body, up to ca 42 km across (east of Devoncourt homestead) and a much smaller triangular shaped lobe (ca 4.5 km2 around Dronfield railway siding). Geochron is a new SHRIMP zircon Pb/Pb magmatic crystallisation age from an outlying area and two previous ages [from the main body]. Associated with several small Cu and Au prospects and abandoned mines. Characterised by anomalously low K2O and Rb, and high Na2O and Sr contents compared to most granites.|1518 +/- 5 Ma, 1508 +/- 4 Ma, 1512 +/- 4 Ma||||Includes biotite granite, and unfoliated but extensively altered granite.|
27935|Wimberu Granite|72949|6|Mentioned|p35|Calymmian|Calymmian|Mount Isa Inlier, Western Fold Belt.||||||
27935|Wimberu Granite|73083|6|Mentioned|p63|||||||||
27935|Wimberu Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1512 +/- 4 Ma, 1508 +/- 4 Ma|||||
27935|Wimberu Granite|73553|4|Described|p40, p59, p150-151,|Calymmian|Calymmian|Of the Williams Batholith. Large intrusive complex up to ~42 km across, a much smaller lobe has also been mapped 20km to the west. Forms low bouldery hills and rises interspersed with very poor outcrop. Mainly mottled pale green tones on radiometric images, very high response on aeromagnetic images. U-Pb LA-ICP-MS titanite age of 1504+/-3.2 Ma interpreted as a titanite recrystallisation age (Murphy, 2020). Assigned to Squirrel Hills Suite by Wyborn (1998). Member of the Williams Supersuite of Budd et al., (2001). See also p164, p221, p259-266.|1518+/-5 Ma, 1508+/-4 Ma U-Pb (SHRIMP) zircon|Williams Supersuite, Squirrel Hills Suite||Intrudes Bulonga Volcanics, Argylla Formation, unconformably overlain by Mount Birnie beds|Includes altered, pale pink, medium-grained, slightly porphyritic amphibole-clinopyroxene granite, sparse plagioclase phenocrysts; fine grained, slightly-moderately porphyritic biotite-amphibole quartz monzonite; generally non-foliated.|03-FEB-23
24109|Wimma Sandstone Member|13497|4|Described|v, vi, viii, xii, p69 fig 6.1|Anisian|Scythian|Cooper Basin. Originally defined by Powis (1989) before being redefined by Channon and Wood (1989). Reference sections nominated by Powis (1989) and Channon and Wood (1989). More than 100m thick in the Patchawarra trough and reaches a maximum thickness of 114m in Potiron 1. Petrography is briefly discussed. Reservoir and outcrop characteristics are discussed. Deposited by low-sinuosity river systems. See also p104-p105, p110-p112, p157 tbl 10.1, p159, p161, p166, p167 fig 10.10.||Arrabury Formation||Equivalent to the Paning Member. Overlies the Callamurra Member and the Paning Member. Conformably overlain by the Tinchoo Formation.|Buff to pale grey, fine to medium-grained quartzose sandstone with minor interbeds of pale to medium grey siltstone and mudstone.|
24109|Wimma Sandstone Member|13516|5|Briefly described|p171 fig 12|Early Triassic|Early Triassic|In Eromanga Basin.||Of Arrabury Formation||||
24109|Wimma Sandstone Member|22839|6|Mentioned|P33|||||||||
24109|Wimma Sandstone Member|22883|6|Mentioned|P29|||Parent is Arrabury Formation.||||||17-SEP-08
24109|Wimma Sandstone Member|23155|6|Mentioned|Fig 8 on p16|||||||||
24109|Wimma Sandstone Member|23375|4|Described|Fig2 p265,280||Spathian|Of the Arrabury Formation. Geological province: Cooper Basin.||||||17-JAN-08
24109|Wimma Sandstone Member|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Early Triassic|Of the Arrabury Formation (Nappamerri Group).  Geological Province: Cooper Basin.||||||
24109|Wimma Sandstone Member|42008|3|Fully described|PP271|Anisian|Scythian|Of the Arrabury Formation.||||||17-JAN-08
24109|Wimma Sandstone Member|42085|6|Mentioned|Fig.2 P374|||||||||
24109|Wimma Sandstone Member|43628|6|Mentioned|Fig.13|||||||||
24109|Wimma Sandstone Member|44133|5|Briefly described|p65 Fig. 8.3, 86|Triassic|Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin. Overlies: Paning Member ). Overlain by the Tinchoo Formation.||||||
24109|Wimma Sandstone Member|60717|5|Briefly described|p40 Fig. 2|Anisian|Scythian|Of Arrabury Formation (Nappamerri Group). Overlies and interfingers with Paning Member of the same unit. Thickness: 100m. Geological Province: Cooper Basin.||||||31-JAN-08
24109|Wimma Sandstone Member|61613|5|Briefly described|p282 Fig. 2|Early Triassic|Early Triassic|Sandstone is Sst in Fig. 2. Of Arrabury Formation. Overlain by Doonmulla Member, Underlain by Paning Member. Geological Province: Cooper and Simpson Basins.||||||18-JUL-14
24109|Wimma Sandstone Member|61615|6|Mentioned|p302 Fig. 2|Middle Triassic|Early Triassic|Of Nappamerri Group. Geological Province: Cooper Basin.||||||07-FEB-11
24109|Wimma Sandstone Member|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Early Triassic|Of Arrabury Formation. Geological Province: Cooper Basin.||||||
24109|Wimma Sandstone Member|62730|5|Briefly described|p352 Fig. 1|Middle triassic|Early Triassic|Of the Arrabury Formation. Geological Province: Cooper Basin.||||||21-APR-08
24109|Wimma Sandstone Member|63978|2|Defined|p22, Fig. 3|Middle Triassic|Early Triassic|Of Powis (1989). Of Arrabury Fm. Conformable on Paning Mbr; unconformable below Tinchoo Fm. Mainly finely interbedded sandstone with pale to medium grey siltstone; mudstone is buff to pale grey, fine- to medium-grained, quartzose. In the Cooper Basin.||||||07-FEB-11
24109|Wimma Sandstone Member|64048|5|Briefly described|p67|||Within the upper Arrabury Formation. Consists dominantly of fine- to medium-grained quartzose sandstone with minor interbeds of medium-grey siltstone and mudstone. Contains oil.||||||07-FEB-11
24109|Wimma Sandstone Member|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Early Triassic|Appears only as Wimma in Fig.1c. Cooper Basin||Unit in Arrabury Group.||Overlies Paning Member. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Cooper Basin.||Top unit in Arrabury Formation.||Overlies Paning Member.||
24109|Wimma Sandstone Member|65489|5|Briefly described|p48, p96, p131-132|Anisian|Scythian|100m thick. Hosts economic oil and gas reservoirs.||Topmost unit in Arrabury Formation.||Overlies Paning and Callamurra Members. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|67402|5|Briefly described|p90, p90 fig CPR4|||Probably a facies equivalent of the Paning Member. Deposited in a fluvial environment. Generally regarded as a poor-quality reservoir but may form a structural trap. Generally greater than 100m thick. See also p91 tbl CPR1, p94, p99 fig CPR14, p100, p101, p101 tbl CPR2, p105.||Arrabury Formation||Conformably overlies the Paning Member. Unconformably overlain by the Doonmulla Member.|Stacked medium to fine-grained sandstones with finely interbedded siltstones and mudstones.|
24109|Wimma Sandstone Member|68731|5|Briefly described|p200 Fig 3.110, p207, pp209-211|Middle Triassic|Lower Triassic|Cooper Basin. Powis (1989). Up to 100 m thick. Deposition occurred in weakly sinuous rivers. Limited palynological data indicate late Olenekian-early Anisian (Gray and McKellar 2002).||Of the Arrabury Formation.||Unconformably overlain by the Tinchoo Formation. Conformably underlain by the Paning Member.|Comprises fine to medium, quartzose sandstone with minor interbeds of siltstone and mudstone.|
24109|Wimma Sandstone Member|69797|5|Briefly described|p17 Fig.2|Middle Triassic|Early Triassic|Age: Scythian - Anisian (approximated from figure). Geol. Prov: Cooper Basin.||Arrabury Formation||||
24109|Wimma Sandstone Member|69946|5|Briefly described|p9, p36, p54|Anisian|Scythian|Cooper Basin.||Unit in Arrabury Formation.||Overlies Paning Member. Is overlain by Doonmulla Member (Tinchoo Formation).||
24109|Wimma Sandstone Member|69947|5|Briefly described|p13 Fig.7.2|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||||
24109|Wimma Sandstone Member|70317|6|Mentioned|p33|Middle Triassic|Early Triassic|Cooper Basin.||Arrabury Formation.||Overlies Paning and Callamurra Members. Is overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|70823|5|Briefly described|p40, p75-p76, p79, p81|||Cooper Basin. Contains economic oil and gas reservoirs locally.||Arrabury Formation||Overlies the Callamurra and Paning Members.|Sandstone with minor siltstone interbeds.|
24109|Wimma Sandstone Member|70824|4|Described|p7, p104|Olenekian|Olenekian|Cooper Basin. Deposited in braided fluvial channels and floodplain environments.||Arrabury Formation||Conformably overlies the Paning Member. Overlain by the Tinchoo Formation.|Sandstone with minor siltstone interbeds.|
24109|Wimma Sandstone Member|70946|5|Briefly described|p1089|Middle Triassic|Early Triassic|Cooper Basin. Deposited in a braided fluvial channel belt and floodplain environment.||Arrabury Formation.||||08-OCT-18
24109|Wimma Sandstone Member|71342|6|Mentioned|Ch5 p9, Ch5 p36, Ch5 p54, Ch7 p13|Anisian|Scythian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a braided fluvial channel or floodplain environment.||Arrabury Formation||Overlies the Paning Member. Overlain by the Tinchoo Formation.||
24109|Wimma Sandstone Member|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin. Contains oil and gas.||Nappamerri Group||||
24109|Wimma Sandstone Member|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin.  Along with Callamurra Member, Panning Member and Tinchoo Formation, shown as floodplain, lacustrine, fluvial channels. Oil and gas.||||||
24109|Wimma Sandstone Member|73251|6|Mentioned|p62|Middle Triassic|Early Triassic|Cooper Basin. Braided fluvial channel belt and floodplain depositional environments. Contains[?] gas and oil.||Arrabury Formation, Nappamerri Group||Underlain by Callamurra Member. Underlain by and equivalent to Paning Member. Overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin. Hosts oil and gas.||Nappamerri Group||Underlain by Panning Member. Overlain by Tinchoo Formation.||
24109|Wimma Sandstone Member|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment.|ca 241 Ma|Nappamerri Group||Overlies Panning Member, underlies Tinchoo Formation||
41105|Wind Mill Diorite|50301|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
41105|Wind Mill Diorite|65388|2|Defined|p278, p236, p237, 238, 249, 256, 262|Early Permian|Late Carboniferous|Intrudes the Torsdale Volcanics. Interpreted as older than Dawson Granite. Inferred to pre-date Glen View Quartz Monzodiorite, J P Granite. Age uncertain. Dark grey gabbro to pale grey quartz diorite.||||||
41105|Wind Mill Diorite|68679|5|Briefly described|p406-408|||Auburn Subprovince, New England Orogen. Is cut by unnamed granite and granodiorite units.||||Intrudes Torsdale Volcanics.|Grey gabbro to quartz diorite; locally gabbro and diorite occur in net-vein association with granite. Locally well-developed igneous foliation.|
24112|Windorah Formation|23982|6|Mentioned|p97 Appendix 13|||Geological Province: Great Artesian Basin.||||||
24112|Windorah Formation|42496|3|Fully described|p142|||Reserved 1986, V.Passmore.||||||
24112|Windorah Formation|42520|5|Briefly described|p6|||||||||
36456|Windsor Granite|23430|5|Briefly described|p495|||||||||
38211|Windsor Supersuite|23422|5|Briefly described|p208 Table 6.4|Ordovician|Cambrian|||||||
38211|Windsor Supersuite|63154|5|Briefly described|p285 Fig. 5|Ordovician|Ordovician|Geological province: Charters Towers Province.||||||
35005|Wingfield Granite|23037|6|Mentioned|p15,6,44-7,87-90,129,139|Early Triassic|Late Permian|Replaces Wingfield Adamellite.||||||
35005|Wingfield Granite|24488|5|Briefly described|Map Legend|Triassic|Triassic|||||||
35005|Wingfield Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgwi].  Typically grey and pink. porphyritic hornblende-biotite granite with large pink K-feldspar phenocrysts up to 4cm; locally pale grey to pink, biotite-hornblende granite with mumerous mafic xenoliths.||||||
35005|Wingfield Granite|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|Overlain by Precipice Sandstone.||||||17-MAY-04
35005|Wingfield Granite|60282|5|Briefly described|p8, p18|||Largest granitoid unit in the Rawbelle Batholith.  Probably supersedes Wingfield Adamellite.  See also p21.||||||13-APR-05
35005|Wingfield Granite|61087|5|Briefly described|Map Legend|Early Triassic|Late Permian|Typically pale grey and pink, porphyritic hornblende-biotite granite with large pink K-feldspar phenocrysts up to 4cm; locally pale grey to pink biotite-hornblende granite with numerous mafic xenoliths.||||||
35005|Wingfield Granite|65388|2|Defined|p336-338, 13, 39, 42, 208, 237, 238,301|Early Triassic|Early Triassic|Of Wingfield Suite. Appears to be one of the youngest intrusives in the region. Has slivers of gneissic rock along western margin. Geochemistry suggests may be composite unit. Inferred to intrude Yaparaba Volcanics, Camboon Volcanics. Intrudes Nogo beds. Partly overlain by Muncon Volcanics. Other relationships unclear. Early to Middle Triassic ages ranging from 233 to 247Ma (recalculated to IUGS constants) may be partly reset.  SHRIMP U-Pb zircon dating gave an age 251.1+/- 3.6Ma. Most commonly porphyritic granite or granodiorite. See also p303, 304, 318, 319, 323, 339-340.||||||
35005|Wingfield Granite|68008|5|Briefly described|p67, p193-194, p292, p432, p435|||Geophysics contrasted with Kariboe Gabbro. Ages from hornblende and biotite respectively.|247 +/- 5 Ma and 240 +/- 5 Ma (K-Ar).|||Intrudes Lochenbar Formation. Abuts (possibly intrudes) Kariboe Gabbro. Is overlain nonconformably by Muncon Volcanics.|Granodiorite.|
35005|Wingfield Granite|68679|4|Described|p410, p416-417, p419-420|||Most extensive unit (~1415 km2) in the Rawbelle Batholith, southern part of the northern New England Orogen. Geochemistry plot. This age is considerably older than previous determinations by Webb and McDougall (1968) of ~247-233 Ma.|251.1 +/- 3.6 Ma (SHRIMP: Fanning et al., 2009).|Wingfield Suite.||Steeply abuts Harrami Igneous Complex. Intrudes Yaparaba and Camboon Volcanics.|Porphyritic hornblende-biotite granite to granodiorite with large (up to 4 cm) irregularly distributed K-feldspar megacrysts, quartz monzonite to quartz monzodiorite, and porphyritic (hornblende) hornblende-biotite granodiorite.|
35005|Wingfield Granite|69594|6|Mentioned|p561|||Rawbelle Batholith.||||||
35005|Wingfield Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|251+/-3.6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
77819|Wingfield Suite|65388|4|Described|p339-340, 284, 287, 295-298, 300|Early Triassic|Late Permian|Rawbelle Batholith. I-type. Includes Cheltenham Creek Granite, Colodon, Euroka , Pollard Granodiorites, Wingfield Granite. See also Winfield Suite in figs p281-283. Geophysical images similar to Coonambula Granodiorite, but geochemistry distinct. Geochemistry overlaps with Tandora Suite but has distinctive elements. Also compared with Tecoma Granite. See also p318, 333, 447. ||||||
77819|Wingfield Suite|68553|6|Mentioned|Map legend; schematic diagram.|Early Triassic|Late Permian|This unit, as well as the Harrami Igneous Complex, the Tandora Suite, the Delubra Gabbro, and various unnamed plutonic units in the Rawbelle Batholith, are all mapped under the symbol, PRgr.||||||30-SEP-15
77819|Wingfield Suite|68679|5|Briefly described|p312, p416, p418-420|Early Triassic|Permian|Withnall et al. (2009). Rawbelle Batholith, northern New England Orogen. Geochemistry plot.|||Colodon, Euroka, Pollard Granodiorites; Cheltenham Creek, Wingfield Granites.|||
30711|Winston Churchill Granite|24197|5|Briefly described|p28, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite (part of the Wonga Batholith). Intrudes the Argylla Formation. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
30711|Winston Churchill Granite|50536|5|Briefly described|p1.4, 5.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Wonga Suite.||||||07-NOV-08
30711|Winston Churchill Granite|73553|4|Described|p64-67, p70, p74 Tb 4.1.2, p228|Statherian|Statherian|Argylla Igneous Province intrusion. Elongate north to NNW-trending body. Formerly mapped as Wonga Granite subunits '1b' and '1ba', later divided and named (Bastrakova et al., 2001) but still included in the Wonga Suite (Budd et al., 2001). Separated from Wonga Igneous Subprovince in this study based on age difference. Only prior description by Bastrakova et al., (2001). Low magnetic response relative to Argylla Formation. Bright blue to white tones on radiometric images. A-type. Misspelt as Chruchill Granite p228.|1778+/-3 Ma zircon U-Pb SHRIMP|||Interpreted to intrude Argylla Formation, intruded by Lakeview Dolerite|Deeply weathered, strongly foliated biotite granite, locally porphyritic. Pink coarse-grained K-feldspar foliated granite cross-cut by minor mafic and aplitic dykes.|
38867|Winterbourne Volcanics|24488|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38867|Winterbourne Volcanics|24489|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38867|Winterbourne Volcanics|24615|5|Briefly described|CD|Triassic|Triassic|[Rvw].  Rhyolite, trachyte, ignimnbrite, rhyolitic breccia, tuff, minor basalt.||||||
38867|Winterbourne Volcanics|50197|5|Briefly described|Map Legend|Triassic|Triassic|||||||
38867|Winterbourne Volcanics|50214|5|Briefly described|Map Legend|Early Triassic|Early Triassic|||||||
38867|Winterbourne Volcanics|60282|6|Mentioned|p11|Triassic|Triassic|Sequence of rhyolite, rhyolitic ignimbrite, agglomerate and breccia with only minor amount of basic lavas.||||||
38867|Winterbourne Volcanics|65388|6|Mentioned|p208, 209|Triassic|Triassic|Overlain by Precipice Sandstone in Mulgildie Basin.||||||
38867|Winterbourne Volcanics|65452|5|Briefly described|p2-4, p35|Late Triassic|Late Triassic|Occupies Kroombit Tops Caldera. Mafic to intermediate volcanism followed by significant periods of voluminous silicic magmatism and development of large caldera system.|218 +/- 3 Ma (Rb-Sr whole rock).||||Basaltic to andesitic lavas, andesitic breccia, ash, crystal and crystal-lithic tuffs at base; rhyolitic and trachytic lava and pyroclastics above; overlain by rhyolitic ignimbrite, breccias and tuffs, higher proportion of breccia.|
38867|Winterbourne Volcanics|67203|6|Mentioned|p2-3, p36-37|Late Triassic|Late Triassic|Murray et al., (in prep). Associated with caldera complex. Further geochronological and geochemical work may determine the width of this Late Triassic volcanic belt.||||||
38867|Winterbourne Volcanics|67874|5|Briefly described|p2-3, p30-33, p37-40, p50-51|Late Triassic|Late Triassic|Forms the elevated and densely vegetated plateau of Kroombit Tops. Originally considered Early to Middle Triassic; later given a Late Triassic Rb-Sr whole rock age of 218 +/- 3 Ma (Murray et al.). SHRIMP U-Pb zircon magmatic crystallisation age.|227.3 +/- 1.4 Ma (Cross et al., 2012).||||A lower eruption sequence dominated by basaltic to andesitic lavas and pyroclastic deposits, and an upper eruption sequence dominated by rhyolitic lavas, ignimbrites, breccias and tuffs.|
38867|Winterbourne Volcanics|68008|2|Defined|p48, p64, p132, p200-210, p213-214|Late Triassic|Late Triassic|See also p227-228, p233, p416, p530-531, p565. Named and defined in this article. Previously included in the Muncon Volcanics by Dear (1968). Kroombit Tops and Blue Hills homestead area. Named after Parish of Winterbourne in which typical rocks crop out. The type section has two parts, for the lower and upper parts of the caldera eruption sequence: Biloela sheet GR283850 7294650 to GR288000 7293200, and GR290300 7202200 to GR294400 7304950 respectively. Variable thickness up to 270m. Is overlain by Annie Creek beds and unconformably by Precipice Sandstone. Geophysical responses described. Lithology and eruption history detailed. Some rhyolites have similar geochemistry with Coulston Volcanics. Other similar U-Pb zircon and Rb-Sr ages given.|224.1 +/- 1.3 Ma; 215.1 +/- 0.7 Ma.|||Unconformably overlies Rockhampton Group, Marble Waterhole beds, Lochenbar and Mount Alama Formations, Three Moon and Youlambie Conglomerates. May be correlated with Coulston Volcanics. See Comments.|Lower eruption sequence has basalt to andesite, including lavas and pyroclastic deposits: breccia, tuff and minor ignimbrite; then rhyolitic and trachytic lava and pyroclastics. Upper sequence has rhyolite, rhyolitic ignimbrite, breccias and tuffs.|
38867|Winterbourne Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera and Portal Creek Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
38867|Winterbourne Volcanics|68679|5|Briefly described|p312-313, p316, p338, p434, p442-443|Late Triassic|Late Triassic|See also p444 Fig.5.104. Kroombit Tops area, northern New England Orogen. Similar to Dooloo Tops Volcanics.|227.3 +/- 1.4 Ma (SHRIMP: Cross et al., 2012).|||Unconformably overlies Marble Waterhole beds. Is overlain by Precipice Sandstone (remnants).|Mainly lower basaltic to andesitic lavas and pyroclastics, and upper rhyolitic lavas, ignimbrites, breccias and tuffs. Also intensely welded to rheomorphic, columnar-jointed ash-rich ignimbrites.|
38867|Winterbourne Volcanics|71592|5|Briefly described|Appendix A.||||227+/-1.4 Ma (SHRIMP U-Pb zircon).||||Ignimbrite.|
38867|Winterbourne Volcanics|73450|4|Described|p3-4, p11-12, p26|Norian|Carnian|Forms the topographic high plateau of Kroombit Tops and Dooloo Tops. Ignimbrites are locally columnar-jointed and intensely welded to rheomorphic (lava-like) indicating high temperature and/or low viscosity compositions. Yielded a U-Pb SHRIMP zircon age of 227.3 +/- 1.4 Ma from a dacitic ignimbrite (Cross et al., 2012). Possibly correlated to Mount Eagle Volcanics.|227.3 +/- 1.4 Ma U-Pb SHRIMP||||Includes a lower eruption sequence dominated by basaltic to andesitic lavas and pyroclastic deposits and an upper sequence dominated by rhyolitic lavas, ignimbrites, breccias and tuffs.|
29755|Wipella Granodiorite|23420|4|Described|p 152 table 4.8||Early Devonian|In the Wipella Suite of the Kintore Supersuite.||||||
29755|Wipella Granodiorite|43596|4|Described|p34|||Of Wipella Suite. Also informally referred to here as Wipella Granite (27 Tb. 3). Intrudes Dinah Formation and possibly the Watch branch Monzogranite. Granodioritic to tonalitic in composition, with an abundantly quartz-phyric texture.||||||27-JAN-09
29755|Wipella Granodiorite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
29754|Wipella Suite|23420|4|Described|p 152 table 4.8||Early Devonian|Also see p 148 table 4.7. In the Kintore Supersuite, Cape York Penninsula Batholith.||||||
29754|Wipella Suite|43596|4|Described|p34, p27 Tb. 3|||Of Kintore Supersuite. Consists of a single pluton, the Wipella Granodiorite; also informally referred to here as Wipella Granite.||||||27-JAN-09
29754|Wipella Suite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kintore Supersuite||||||24-JAN-05
69503|Wireyard Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Pale pink, fine to medium-grained, even-grained to porphyritic biotite granite.|
25638|Wirra Volcanic Subgroup|23291|4|Described|p40, p95 Tb. 3.10|Permian|Carboniferous|Parent: Newcastle Range Volcanic Group. Geological Province: Georgetown Region.||||||26-MAY-15
25638|Wirra Volcanic Subgroup|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
25638|Wirra Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p3.||Carboniferous|||||||
25638|Wirra Volcanic Subgroup|43740|5|Briefly described|p7|||||||||
25638|Wirra Volcanic Subgroup|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group. Includes the Bousey Rhyolite.||||||26-MAY-15
25638|Wirra Volcanic Subgroup|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Newcastle Range Volcanic Group. Consists of the Bousey Rhyolite and Jinker Creek Rhyolite.||||||26-MAY-15
25638|Wirra Volcanic Subgroup|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Newcastle Range Volcanic Group.|Includes Bousey and Jinker Creek Rhyolites.||Mainly rhyolitic ignimbrite.|
25638|Wirra Volcanic Subgroup|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Newcastle Range Volcanic Group.|Includes Bousey Rhyolite.||Buff to purple, crystal-rich rhyolitic ignimbrite (25% quartz and feldspar crystals).|
25638|Wirra Volcanic Subgroup|68576|5|Briefly described|Q_11: p21|Carboniferous|Carboniferous|Forms the Wirra Cauldron.||Newcastle Range Volcanic Group.||||
25638|Wirra Volcanic Subgroup|70207|5|Briefly described|p14, p81-82|||Georgetown region. Other age determinations discussed.|318 +/- 4 Ma (Rb-Sr: Black, 1973).|Newcastle Range Volcanic Group.|Bousey Rhyolite.|||
79958|Wirrega Granite|71965|6|Mentioned|p911|||Geological province: Thomson Orogen. Of Ella Belt.||||||
74961|Woin-Garin Suite|60425|4|Described|p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Of Dunk Island Supersuite. Contains Woin-Garin Suite. I-type.||||||07-FEB-11
74960|Woin-Garin granite|60425|4|Described|p98, p100, p288-9 Appdx.|Early Carboniferous|Early Carboniferous|Informal name. Of Woin-Garin Suite (Dunk Island Supersuite).Age:336+/-5ma (SHRIMP).White to brown (altered), med.to coarse-grained, mod'ly porph.biotite granite;+well-dev'd tectonic foliation, numerous enclaves of mainly microdiorite(?), + biotite gneiss||||||07-FEB-11
24117|Wolca Granite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
24117|Wolca Granite|39505|6|Mentioned|p167|||||||||
24117|Wolca Granite|39997|6|Mentioned|p165|||||||||
24117|Wolca Granite|41778|2|Defined|Table 1|Permian||Described p370.||||||30-SEP-08
24117|Wolca Granite|42054|6|Mentioned|p273|||||||||
24117|Wolca Granite|43008|5|Briefly described|map legend|||||||||
24117|Wolca Granite|63821|5|Briefly described|p28|Late Permian|Early Permian|Age: 261+/-4Ma and 254+/-5Ma (K-Ar biotite) Intrudes Curtis Island Group; intruded by Wonbah Granodiorite and Nour Nour Granodiorite. Several different phases, incl. very coarse granite with large zoned plagioclase crystals, granodiorite + quartz diorite.||||||07-FEB-11
24117|Wolca Granite|65452|5|Briefly described|p7 Tb.2|Guadalupian|Guadalupian|SHRIMP U-Pb zircon magmatic crystallisation age.|262.9 +/- 1.6 Ma (Carson et al. 2006).||||Melanocratic biotite granodiorite.|
24117|Wolca Granite|68679|5|Briefly described|p410, p421-422|||Gayndah-Gladstone belt, southern part of the northern New England Orogen.|262.9 +/- 1.6 Ma (SHRIMP: Carson et al., 2006).|||Adjacent to Tenningering Granodiorite.|Coarsely K-feldspar-phyric biotite (rapakivi) granite, hornblende-biotite granodiorite and hornblende-biotite tonalite. Lithologically variable but probably entirely I-type.|
24117|Wolca Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|263+/-1.6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
34976|Wolfang Conglomerate|23008|6|Mentioned|p460|||||||||
23239|Wollenden Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Wakara Volcanic Subgroup of Featherbed Volcanic Group.||||||
23239|Wollenden Rhyolite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup.||||||
23239|Wollenden Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup & Lags Supersuite.||||||
23239|Wollenden Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V105. A-Type.||||||
23239|Wollenden Rhyolite|23616|5|Briefly described|Table 3 p46||Permian|Of Wakara Volcanic Subgroup. Hodgkinson Province.||||||
23239|Wollenden Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
23239|Wollenden Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Wakara Volcanic Subgroup.||||||
23239|Wollenden Rhyolite|43259|4|Described|Appendix 1,p10.||Early Permian|of Wakara Volcanic Subgroup.||||||
23239|Wollenden Rhyolite|43626|2|Defined|p72||Early Permian|Age between 289+/-10 Ma and 278+/-3 Ma||||||
23239|Wollenden Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
23239|Wollenden Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
23239|Wollenden Rhyolite|60425|5|Briefly described|p44 Tb. 3|Early Permian|Early Permian|Informal subunit of Wakara Volcanic Subgroup (Featherbed Volcanic Group). Unconformably overlies Yongala Volcanic Subgroup units.||||||07-FEB-11
23239|Wollenden Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province. Each variant is mapped separately.||Unit in Wakara Volcanic Subgroup.|||Flow-banded, slightly porphyritic rhyolite; intensely welded, crystal-rich rhyolitic ignimbrite; massive volcanic breccia; intensely welded, lithics-poor, crystal-rich, rhyolitic ignimbrite with rare garnet and 'pumice' fragments.|
24118|Womblealla Rhyolite Member|23291|4|Described|p92 Fig. 3.9|Early Permian|Late Carboniferous|Parent: Ironhurst Formation of the Maureen Volcanic Group. Thickness: 200-250m. Geological Province: Georgetown Region.||||||08-JUL-15
24118|Womblealla Rhyolite Member|23510|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|of Ironhurst Formation, Maureen Volcanic Group.||||||
24118|Womblealla Rhyolite Member|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
24118|Womblealla Rhyolite Member|40542|6|Mentioned|p97|||||||||
24118|Womblealla Rhyolite Member|43259|6|Mentioned|Appendix 1,p1.||Carboniferous|||||||
24118|Womblealla Rhyolite Member|43740|6|Mentioned|Fig.5,p45|||||||||
24118|Womblealla Rhyolite Member|50595|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Ironhurst Formation. Overlies: Ant Hill Andesite Member. Underlies: Puranga Rhyolite.||||||24-JUN-15
24118|Womblealla Rhyolite Member|68352|5|Briefly described|Map legend.||Late Carboniferous|Kennedy Province. Maureen Cauldron. Age min: Early Permian?||Unit in Ironhurst Formation.||Conformably overlies Ant Hill Andesite Member. Is overlain conformably by Puranga Rhyolite.|Greyish-brown, crystal-poor to crystal-rich, rhyolitic ignimbrite with abundant lithic clasts; strongly flow-banded rhyolite, locally autobrecciated.|19-MAY-15
26230|Wonbah Granodiorite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
26230|Wonbah Granodiorite|41738|6|Mentioned|p168|||||||||
26230|Wonbah Granodiorite|41778|2|Defined|Table 2|Cretaceous|Jurassic|||||||
26230|Wonbah Granodiorite|43008|5|Briefly described|map legend|||||||||
26230|Wonbah Granodiorite|63821|4|Described|p28, p32|Late Triassic|Late Triassic|Age: 219Ma (K-Ar hornblende), 225Ma (K-Ar biotite). Intrudes Wolca and Tenningering Granites and New Moonta Diorite. Comprises hornblende-biotite granodiorite, altered hornblende-biotite granodiorite and hornblende-biotite granodiorite to quartz diorite.||||||07-FEB-11
26230|Wonbah Granodiorite|64556|6|Mentioned|p56|Late Triassic|Late Triassic|||||||07-FEB-11
26230|Wonbah Granodiorite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
26230|Wonbah Granodiorite|68679|5|Briefly described|p431|||Other ages given.|219 Ma (K-Ar hornblende: Webb and McDougall, 1967)|||Adjacent to Moolboolaman Granodiorite.|Hornblende-biotite granodiorite with a marginal phase of medium-grained hornblende-biotite quartz diorite.|
26230|Wonbah Granodiorite|73450|6|Mentioned|p24-25|Norian|Norian|A U-Pb SHRIMP zircon age of 224 +/- 1.3 Ma was reported by Carson et al. (2007).|224 +/- 1.3 Ma U-Pb SHRIMP|||Intruded by Hogback Granite.||
27938|Wonga Granite|22522|6|Mentioned|Fig2p332,Fig3p333|||||||||
27938|Wonga Granite|22623|6|Mentioned|p226|||||||||
27938|Wonga Granite|22722|6|Mentioned|p272|||||||||
27938|Wonga Granite|23071|5|Briefly described|p760|Statherian|Statherian|||||||
27938|Wonga Granite|23192|6|Mentioned|Fig.2|||||||||
27938|Wonga Granite|23324|5|Briefly described|p468 Fig.1|||Metagranitic gneiss.||||||07-FEB-07
27938|Wonga Granite|23458|5|Briefly described|p114, p121|||Part of the Wonga Batholith.||||||27-AUG-07
27938|Wonga Granite|23545|5|Briefly described|Fig 1 p604|||||||||
27938|Wonga Granite|23967|6|Mentioned|p1331 Fig.1|||||||||
27938|Wonga Granite|24197|6|Mentioned|p14 Fig. 1.3.2a|Proterozoic|Proterozoic|Geological province: Mount Isa Block.||||||07-FEB-11
27938|Wonga Granite|24253|6|Mentioned|p6|||Geological Province: Mount Isa Block.||||||
27938|Wonga Granite|24254|5|Briefly described|p23|Proterozoic|Proterozoic|Age: ca. 1740-1730 Ma. Geological Province: Mount Isa Inlier.||||||
27938|Wonga Granite|24255|5|Briefly described|p32 Fig.1, p33 Fig.2|Statherian|Statherian|Geological Province: Eastern Succession, Mount Isa Block. Age: granite gneiss 1750-1740 Ma.||||||
27938|Wonga Granite|24256|6|Mentioned|p50 Fig.2|||Geological Province: Mount Isa Block.||||||
27938|Wonga Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
27938|Wonga Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
27938|Wonga Granite|24259|6|Mentioned|p105|||Geological province: Mount Isa Block.||||||
27938|Wonga Granite|29550|5|Briefly described|p44|||||||||
27938|Wonga Granite|30527|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27938|Wonga Granite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
27938|Wonga Granite|30531|6|Mentioned|p20|||Also mention p22.||||||04-MAR-13
27938|Wonga Granite|30536|6|Mentioned|p100|||||||||
27938|Wonga Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27938|Wonga Granite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27938|Wonga Granite|32660|5|Briefly described|Table 5|||||||||
27938|Wonga Granite|32959|6|Mentioned|Fig.21|||||||||
27938|Wonga Granite|33900|6|Mentioned|p9|||||||||
27938|Wonga Granite|35074|6|Mentioned|Fig.2|||||||||
27938|Wonga Granite|35139|6|Mentioned|p10|||||||||
27938|Wonga Granite|35167|6|Mentioned|p154|||||||||
27938|Wonga Granite|35286|4|Described|p145|||||||||
27938|Wonga Granite|35932|6|Mentioned|p452|||||||||
27938|Wonga Granite|35950|6|Mentioned|p305|||||||||
27938|Wonga Granite|36052|4|Described|p419|||Discussed throughout article.||||||
27938|Wonga Granite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27938|Wonga Granite|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
27938|Wonga Granite|36963|6|Mentioned|p241|||||||||
27938|Wonga Granite|36965|6|Mentioned|p244|||||||||
27938|Wonga Granite|37462|4|Described|Table4.VII|||||||||
27938|Wonga Granite|37565|6|Mentioned|Fig.5|||||||||
27938|Wonga Granite|37568|6|Mentioned|p84|||||||||
27938|Wonga Granite|37862|6|Mentioned|p586|||||||||
27938|Wonga Granite|38276|6|Mentioned|Fig.1|||||||||
27938|Wonga Granite|39445|6|Mentioned|p36|||See also p43 & Table 2. 1671 Ma||||||04-MAR-13
27938|Wonga Granite|39622|6|Mentioned|p26|||See also Appendix||||||
27938|Wonga Granite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
27938|Wonga Granite|39937|6|Mentioned|p82|||||||||
27938|Wonga Granite|40840|6|Mentioned|Map legend|||||||||
27938|Wonga Granite|41031|6|Mentioned|p796|||||||||
27938|Wonga Granite|41465|5|Briefly described|p11|||||||||
27938|Wonga Granite|41744|6|Mentioned|Fig.1|||||||||
27938|Wonga Granite|41979|6|Mentioned|p538|||||||||
27938|Wonga Granite|42201|6|Mentioned|p294|||||||||
27938|Wonga Granite|42365|5|Briefly described|Fig.15 P266|||Probably NOT misspelling of Wonga Complex?||||||
27938|Wonga Granite|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: 1760-1720Ma. Foliated granite, leucogranite.||||||09-FEB-09
27938|Wonga Granite|42781|5|Briefly described|p427|||see also Fig.1 p426, Fig.4 p429.||||||15-MAR-07
27938|Wonga Granite|42858|5|Briefly described|p671|||||||||
27938|Wonga Granite|42859|6|Mentioned|p675|||||||||
27938|Wonga Granite|43615|6|Mentioned|p14|||1730-1760 Ma||||||
27938|Wonga Granite|43616|6|Mentioned|p4|||||||||
27938|Wonga Granite|43643|6|Mentioned|Fig.3,p611|||||||||
27938|Wonga Granite|44271|2|Defined|p37,38,45||Paleoproterozoic|Intrudes Corella Formation.||||||07-NOV-08
27938|Wonga Granite|44275|14|Not recorded|Map Legend|||||||||
27938|Wonga Granite|44276|4|Described|p12,13,map|||||||||
27938|Wonga Granite|44278|4|Described|p5,map|||||||||
27938|Wonga Granite|44526|14|Not recorded|p255|||||||||
27938|Wonga Granite|44751|14|Not recorded|p300||Precambrian|||||||
27938|Wonga Granite|44766|14|Not recorded|p24|||||||||
27938|Wonga Granite|44788|14|Not recorded|p13,16|||||||||
27938|Wonga Granite|44849|14|Not recorded|p69,74,75,82,94|||1450 Ma.||||||
27938|Wonga Granite|44989|2|Defined|p.152-3|||Tb.IV. On many pages. (F54-2,6).||||||
27938|Wonga Granite|45003|14|Not recorded|p17,24,37,39,40|||||||||
27938|Wonga Granite|45087|6|Mentioned|p42|||Chemical analyses||||||
27938|Wonga Granite|45136|3|Fully described|p56|||||||||
27938|Wonga Granite|45166|5|Briefly described|p34|||||||||
27938|Wonga Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
27938|Wonga Granite|46843|6|Mentioned|Fig.2|||||||||
27938|Wonga Granite|46960|6|Mentioned|p217|||||||||
27938|Wonga Granite|46995|6|Mentioned|p269|||||||||
27938|Wonga Granite|46996|6|Mentioned|p273|||||||||
27938|Wonga Granite|48894|6|Mentioned|p32|||Age||||||
27938|Wonga Granite|48906|14|Not recorded|p4|||||||||
27938|Wonga Granite|48997|6|Mentioned|Fig.3|||||||||
27938|Wonga Granite|49041|5|Briefly described|Table 2|||||||||
27938|Wonga Granite|50100|5|Briefly described|p13 Fig.4, p18|Statherian|Statherian|Of the Wonga Suite (Wonga Batholith).  Geological Province: Kalkadoon-Ewen and Easter Fold Belt Provinces.  ||||||
27938|Wonga Granite|50332|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of the Wonga Suite. Age: 1760-1720Ma. Intruded into the Kalkadoon-Ewen Province and Eastern Fold Belt Province. Geological Province: Kalkadoon-Ewen Province and Eastern Fold Belt Province.||||||25-JAN-19
27938|Wonga Granite|50536|5|Briefly described|p11.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1729 +/- 5Ma.||||||07-NOV-08
27938|Wonga Granite|60665|6|Mentioned|p1146|Statherian|Statherian|Premetamorphic.|1750-1730 Ma.|||||
27938|Wonga Granite|61922|5|Briefly described|p17 Fig. 9|Paleoproterozoic|Paleoproterozoic|Intrusive rocks. Age: ~1740Ma. ||||||07-NOV-08
27938|Wonga Granite|61933|6|Mentioned|p169 Fig.3, p177|Paleoproterozoic|Paleoproterozoic|Mentioned in legend only. Age: 1740 Ma.||||||07-NOV-08
27938|Wonga Granite|61963|5|Briefly described|p770 Fig. 1|||||||||
27938|Wonga Granite|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks.||||||
27938|Wonga Granite|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|Palaeoproterozoic|Palaeoproterozoic|600 km2. See also reference to Wonga suite (p287).|ca 1760-1720 Ma.|||||
27938|Wonga Granite|63866|5|Briefly described|p60|Statherian|Statherian|Kalkadoon-Leichhardt and Wonga Belts.|1758 +/- 8 Ma (SHRIMP)|Wonga Suite||||
27938|Wonga Granite|64248|6|Mentioned|p41 Tb.2|||Density range of 2.65-2.68 tonne/m3 used in forward models.||||||
27938|Wonga Granite|64250|6|Mentioned|p9 fig 1, p23 fig 8, p8|||See also entries for Wonga Batholith (not a stratigraphic name): p11 fig 3, p14, p19, p26.|1750 - 1720 Ma.|||||
27938|Wonga Granite|64251|6|Mentioned|p51-52|Paleoproterozoic|Paleoproterozoic|Age: 1800-172-Ma. Geological Province: Mount Isa Inlier.||||||05-MAY-09
27938|Wonga Granite|64726|6|Mentioned|p83 Fig.2.|||||||||
27938|Wonga Granite|64744|5|Briefly described|p353 Fig.4, pp356-357.  |Statherian|Statherian|Mount Isa Basin. Highly strained and variably mylonitised. Intruded by mafic dykes.|c.1780 Ma.|||||
27938|Wonga Granite|65396|5|Briefly described|p23, p53, p78, p172-173, p179, p182,p195|Statherian|Statherian|See also p199, p234-241, p274, p386, p446. Intruded contemporaneously with Cover Sequence 2, Kalkadoon-Leichhardt Belt, Mary Kathleen Fold Belt. Age range also shown as 1750-1720 Ma. Formations with detrital zircons from this unit are listed.|1740 - 1730 Ma|||||
27938|Wonga Granite|65505|6|Mentioned|976, Fig 1-3,7,8|Proterozoic|Proterozoic|Part of the Wonga Suite. Instead of a continuum, it may consist of two separate magmatic episodes: ages of 1778 +/- 3 Ma and 1738 +/- 3 Ma.||||||
27938|Wonga Granite|65755|6|Mentioned|p2|||||||||
27938|Wonga Granite|66529|6|Mentioned|p60, p61  |||The most prospective unit for orthomagmatic U mineralisation in the Mount Isa region.||||||
27938|Wonga Granite|66824|6|Mentioned|p147|||Rb-Sr geochronology age determinations by Page (1978).|1629 +/- 25 Ma; 1621 +/- 28 Ma.|||||
27938|Wonga Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p72|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mary Kathleen Domain, Mount Isa Inlier. Wonga/Burstall Igneous Event. Contains a Zn anomaly. Asterisked as a redundant rock unit name; may be replaced by Breakfast Creek Granite?|1758 +/- 8 Ma.|Wonga Suite, Burstall Suite.|||Strongly foliated to gneissic porphyritic biotite granite.|
27938|Wonga Granite|67498|6|Mentioned|p918 Fig. 1, p919|||Mis-spelling of Wonga Suite? Shown as including Gin Creek Granite in Fig. 1.||||||08-MAY-12
27938|Wonga Granite|68020|6|Mentioned|p128|||||||||
27938|Wonga Granite|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|||||May intrude Marraba Volcanics, Mitakoodi Quartzite, Ballara Quartzite, Corella Formation.||
27938|Wonga Granite|68542|6|Mentioned|p18, p20 fig 6||||1760-1730 Ma|||||
27938|Wonga Granite|68576|5|Briefly described|Q_2: p18, p20|||Appears as Wonga Granite (Gin Creek Granite). Age range is 1760-1730 Ma. Emplaced contemporaneously into Cover Sequence 2.||||||
27938|Wonga Granite|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|Igneous crystallisation age.|1738 +/- 3 Ma|||||
27938|Wonga Granite|69056|6|Mentioned|Time-Space plot sheet;|Statherian|Statherian||1758 +/- 8 Ma.|||||
27938|Wonga Granite|69222|6|Mentioned|p227|||Associated with the Myally Rift Event. Heat production diagram.||||||
27938|Wonga Granite|69370|5|Briefly described|p306-307|Statherian|Statherian|Associated with bimodal volcanics, clastics and carbonate sediments of Cover Sequence 2.|c.1740 Ma (Holcombe et al. 1991)|||Intrudes Overhang Jaspilite, Corella and Doherty Formations.||25-JAN-19
27938|Wonga Granite|69591|5|Briefly described|p36 Fig.2.21, p60|||Wonga Batholith, Mary Kathleen Domain, Mount Isa Province. Another age (not attributed) given is 1738 +/- 3 Ma.|1778 +/- 3 Ma (Neumann et al., 2009).|Wonga Suite.|||Strongly foliated to gneissic porphyritic biotite granite.|
27938|Wonga Granite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Six facies are mapped separately; five are named: "young leucocratic phase", "Rosebud phase", Highway phase", Knob phase", "Wonga Waterhole phase".|||||Strongly foliated to gneissic porphyritic biotite granite and biotite-amphibole metagranite.|
27938|Wonga Granite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Six facies are mapped separately; five are named: "young leucocratic phase", "Rosebud phase", Highway phase", Knob phase", "Wonga Waterhole phase".|||||Strongly foliated to gneissic porphyritic biotite granite and biotite-amphibole metagranite.|
27938|Wonga Granite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Three facies associations are mapped separately.|||||Strongly foliated to gneissic porphyritic biotite granite and biotite-amphibole metagranite.|
27938|Wonga Granite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes three unnamed members: aplite; foliated biotite granite; foliated coarse grained porphyritic biotite granite.|||||Strongly foliated to gneissic porphyritic biotite granite and biotite-amphibole metagranite.|
27938|Wonga Granite|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.|1780-1775 Ma.|||||
27938|Wonga Granite|71592|5|Briefly described|Appendix A.|||Mary Kathleen Domain, Mount Isa Orogen.|1778+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite, gneiss.|
27938|Wonga Granite|72596|6|Mentioned|p2, p24, p46, p56, p63|Statherian|Statherian|Dated sample referred to as Natalie Granite (Geoscience Australia, 2011: Sample ID 72205021)[?]. Also reference to older pluton (1778+/-3 Ma).|1729 +/- 5 Ma, 1758+/-8 Ma|||||
27938|Wonga Granite|72799|6|Mentioned|p40|||Similar in appearance to a low ridge of foliated granite (sampled as DPMI049; this report) from the Boomarra Horst region.||||||
27938|Wonga Granite|73137|6|Mentioned|p1, p95|||Previously tentatively correlated with the Bushy Park Gneiss. [Possible emplacement at 1740 Ma].||||||
27938|Wonga Granite|73413|6|Mentioned|p6, App.1|Statherian|Statherian|U-Pb SHRIMP ages of 1778 +/- 3 Ma and 1738 +/- 3 Ma reported by Neumann et al. (2009). U-Pb TIMS age of 1742 +/- 13 Ma reported by Pearson et al. (1992).|1778 +/- 3 Ma, 1742 +/- 13 Ma, 1738 +/- 3 Ma|||||
27938|Wonga Granite|73553|5|Briefly described|p1, p10, p15, p32, p64, p67, p71-75,|||Wonga Igneous Subprovince. Previously included plutons coeval with the Argylla Igneous Province/Argylla Magmatic Event. Former 'Wonga Granite' was a widespread unit in early regional mapping (Carter et al., 1961), incorporated the Mount Godkin, Burstall, Overlander and Revenue granites. Finer mapping by many authors defined new units and restricted the Wonga Granite to the Wonga Belt with numerous unnamed subunits, and contains a ~1780 Ma component and a ~1740 Ma component. Older units in this study are separated and placed within the Argylla Igneous Province. The former Wonga Granite is divided here based on the units of Bastrakova et al., (2001), remaining areas are grouped into an undivided Wonga Granite unit. See also p81-82, p86, p89, p96, p100-101, p127, p132, p135, p144, p250.|||||Includes undivided foliated, porphyritic to equigranular biotite +/- amphibole monzogranite to syenogranite. Gneissic to strongly foliated.|03-FEB-23
30706|Wonga Suite|23545|5|Briefly described|p603.|||||||||
30706|Wonga Suite|24197|4|Described|p28, p93|Paleoproterozoic|Paleoproterozoic|Granites/volcanics comprising Birds Well and Bushby Park Gneiss + undefined, named units of Wonga Batholith - Mount Maggie, Natalie, Scheelite and Winston Churchill Granites, all intruding Argylla Fm. Geol.Prov: Mount Isa Inlier). Eg.of Sybella Assocn.||||||07-FEB-11
30706|Wonga Suite|50100|5|Briefly described|p11, p18|Proterozoic|Proterozoic|Includes the Wonga and Birds Well Granites and the Bushy Park Gneiss. Intrudes the Corella Formation.||||||15-MAR-07
30706|Wonga Suite|50332|6|Mentioned|p16, p19|Proterozoic|Proterozoic|Includes; Wonga, Natalie and Playboy Granites.||||||07-FEB-11
30706|Wonga Suite|50536|5|Briefly described|p1.2, 1.4, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1760Ma.||||||07-NOV-08
30706|Wonga Suite|63023|6|Mentioned|p1024 Fig. 1|||||||||
30706|Wonga Suite|63866|5|Briefly described|p60|||Wonga Belt.|||Includes the Wonga and Natalie Granites.|Intrudes the Argylla Formation, Ballara Quartzite and Corella Formation.|Coarse-grained, foliated porphyritic granites and gneisses.|
30706|Wonga Suite|65387|5|Briefly described|p84|Statherian|Statherian|Probable source of younger detrital zircons in Knapdale Quartzite and Quamby Conglomerate.|c.1760-1730 Ma (Neumann, 2007).|||||
30706|Wonga Suite|65455|6|Mentioned|p7, p8 Fig. 4|||Mount Isa region, central belt. Granitoids show patchy enrichment.||||||09-MAY-12
30706|Wonga Suite|65505|5|Briefly described|976|Proterozoic|Proterozoic|Includes Wonga Granite. A series of plutons in a N-S belt, 180 km long and up to 20km wide. Coarse-grained foliated porphyritic granite and gneiss. Intrudes Argylla Fm, Ballara Quarzite and Corella Fm. Age: 1742 +/- 13 U-Pb Zircon.||||||
30706|Wonga Suite|66529|6|Mentioned|p65-67|||Temporally, spatially and probably genetically related to the Mary Kathleen U-REE deposit (discussed in some detail). Also appears as Wonga Suite Granites on p61.|~1740-1730 Ma|||||
30706|Wonga Suite|67127|6|Mentioned|p94|||Deposited during the Wonga Extension Event.|ca. 1760 -1720 Ma|||||
30706|Wonga Suite|67323|5|Briefly described|p15, p24, p31, p40, p107|||See also Solid Geology Map. See also Wonga Suite, Burstall Suite. Mary Kathleen Domain. Intruded shear zone and upper plate at ~1740 Ma. Non-magnetic; also has lower gravity than the adjacent Corella Formation. Geochronology, by Neumann et al. (2009), implies two ages for the Suite; the younger part (the Wonga Event) intruding the Corella Formation. |1778 +/- 3 Ma and 1738 +/- 3 Ma.|||Intrudes Argylla and Corella Formations and Ballara Quartzite.||
30706|Wonga Suite|67498|6|Mentioned|p918||||~1750-1730 Ma||Includes Gin Creek Granite?|Intrudes the Soldiers Cap Group.||
30706|Wonga Suite|68542|6|Mentioned|p1, p15|||||||||
30706|Wonga Suite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit, the Burstall Suite and Gin Creek Granite are all mapped under the same symbol, -Pgw.||||||
30706|Wonga Suite|68576|5|Briefly described|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
30706|Wonga Suite|69056|5|Briefly described|p2-6, p53-54, Reference images sheet|Statherian|Statherian|Shown on the simplified surface and solid geology maps of the Quamby Project area. Intrudes the Mary Kathleen and Constantine Domains. Appears as Wonga Supersuite on p4, p6; also Wonga-Burstall Suite on p4-5. Broadly syntectonic: associated with the ~1740 Ma Wonga Event. Coeval with Burstall Suite.|||Dipvale Granodiorite, Levian Granite.||Foliated granitoids.|
30706|Wonga Suite|69591|5|Briefly described|p28, p36|Paleoproterozoic|Paleoproterozoic|Mary Kathleen Domain, Mount Isa Province. Intruded during the Wonga Extension Event (~1755-1740 Ma).|||Wonga Granite.|||
30706|Wonga Suite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.||Includes Birds Well Granite, Bowlers Hole Granite, Bushy Park Gneiss, Mairindi Creek Granite, Myubee Igneous Complex.|Equivalent age to Burstall Suite.|Medium to coarse biotite granite and gabbro, strongly foliated to massive. Foliated biotite-hornblende granite, gneissic -granite. Felsic hornblende-biotite gneiss, augen gneiss. Foliated hornblende-biotite graniteand minor diorite and amphibolite.|
30706|Wonga Suite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.||Includes Birds Well Granite, Bowlers Hole Granite, Bushy Park Gneiss, Mairindi Creek Granite, Myubee Igneous Complex.|Equivalent age to Burstall Suite.|Medium to coarse biotite granite and gabbro, strongly foliated to massive. Foliated biotite-hornblende granite, gneissic -granite. Felsic hornblende-biotite gneiss, augen gneiss. Foliated hornblende-biotite granite and minor diorite and amphibolite.|
30706|Wonga Suite|72889|6|Mentioned|p6 Fig.i., p28|||||||||25-NOV-20
30706|Wonga Suite|73137|6|Mentioned|p90|Statherian|Statherian|Budd et al. (2001) assigned the Birds Well Granite as a constituent.|~1730-1740 Ma||Birds Well Granite|||
30706|Wonga Suite|73413|6|Mentioned|p2-3, p5-6, p20|Statherian|Statherian|Mary Kathleen Domain. [Age written as 1740-1730 Ma, 1780-1720 Ma, ca. 1740 Ma, and 1745-1730 Ma]. Intrudes rocks of Cover Sequence 2 (of Foster and Austin, 2008).|1780-1720 Ma||||May include granites and gabbros.|
30706|Wonga Suite|73529|5|Briefly described|p1, p2 Fig.1, p4, p14-15|Statherian|Statherian|Mary Kathleen Domain, intrudes sedimentary succession. Primarily located in the high strain Wonga Belt, and the Shinfield Zone. Emplacement ages mostly overlap with Burstall Suite. See also Wonga suite granites p14.|1750-1710 Ma|||Intrudes Magna Lynn Metabasalt, Corella Formation|Multi-phase plutons, mylonitic.|
30706|Wonga Suite|73553|5|Briefly described|p1, p15, p19, p64, p132, p243, p246|||Of Budd et al., (2001). Winston Churchill Granite separated from Wonga Suite based on age difference. Formerly included Birds Well Granite [and Bushy Park Gneiss?]. See also 'Wonga Suite, Burstall Suite' p54 [from GIS geological compilation].|||Bushy Park Gneiss|||
29339|Wongella Metamorphics|22845|2|Defined|p12,4,21-5,32,77,80|Early Carboniferous|Late Devonian|Previously mapped as part of the Neara Volcanics.  Correlates with Widgee Metamorphics.||||||
29339|Wongella Metamorphics|22846|6|Mentioned|p20|Carboniferous|Devonian|||||||
29339|Wongella Metamorphics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
29339|Wongella Metamorphics|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
29339|Wongella Metamorphics|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
29339|Wongella Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar and Widgee Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
29339|Wongella Metamorphics|68679|5|Briefly described|p325-328|||Donchak et al. (1995); Tang (2003). Kilkivan-Manumbar area, North D'Aguilar Subprovince. Lower plate accretionary assemblage.||||Is intruded by Coppermine Creek Granodiorite. Structurally underlies Mount Mia Serpentinite. Is faulted against Amamoor beds, Neara Metamorphics. Equivalent to Rocksberg, Peters Creek Greenstones.|Massive to strongly foliated and schistose tremolite-actinolite-chlorite schist, serpentinite, greenschist; characteristic clast-in-matrix tectonic melange fabric, the dominant clast type being altered fine-grained to glassy metabasalt.|
41791|Wongrabry beds|60479|5|Briefly described|Map Legend|Early Permian|Early Permian|Lithic sandstone, conglomerate and mudstone; rare limestone and coquinite.||||||21-OCT-04
41791|Wongrabry beds|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Predominantly andesitic to basaltic volcaniclastic sandstone and conglomerate; subordinate basalt or andesite and rhyolite; rare limestone and coquinite.||||||
41791|Wongrabry beds|61035|5|Briefly described|p12, p13|Permian|Early Permian|Informal name. Geol Prov: Yarrol Province. Contains Early Permian fossils. Consists of volcaniclastic sandstone and conglomerate and some rare limestone.||||||07-FEB-11
41791|Wongrabry beds|65388|3|Fully described|p78-82, 79, 58, 70, 75, 77, 143,445,446|Early Permian |Early Permian |Stoodleigh Subprovince, Yarrol Province. New name from Wongrabry Creek (misspelt Wongabrai), for an area of volcaniclastic sedimentary rocks and lavas previously mapped as Carmila beds and Youlambie Conglomerate (Quail Island). Incomplete type section between MGA 788700 7502600 and MGA 788950 7502600;  Wongrabry beds include Artinskian fossils, hence must be younger than Glenprairie beds.||||||
41791|Wongrabry beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Yarrol Province. This unit, as well as Youlambie Conglomerate and Glenprairie beds, are all mapped under the symbol, CPy.||||||
41791|Wongrabry beds|68679|5|Briefly described|p308, p312-313, p338, p347,p349-350,p359|Cisuralian|Pennsylvanian|Withnall et al. (2009). A ~20km long arcuate belt between Hill End homestead and headwaters of Wellington Creek. Stoodleigh Subprovince, Northern Yarrol Province. High-energy shallow-marine deposits.||||Overlies (locally probably thrust over) Glenprairie beds. May correlate with Berserker Group.|Poorly sorted volcanilithic sandstone with scattered shells or coquinitic layers to 15cm thick; conglomerate and breccia in beds to 10m thick, lithic fragments comprising andesite or basalt, with some rhyolite or dacite; rare basalt lava locally.|
41791|Wongrabry beds|69594|6|Mentioned|p561|Permian|Permian|||||||
28034|Wongu Granite|23420|4|Described|p 151 table 4.8||Early Devonian|In the Aralba Suite of the Kintore Supersuite. Intrudes Yambo Metamorphic Group and Burton Lagoon Granite||||||
28034|Wongu Granite|43596|4|Described|p31, p26 Tb. 2, p28 Tb. 3|||Of Aralba Suite (Kintore Supersuite). Intrudes Oswald and Annie Creek Schists, and Burton Lagoon Granite. Pale grey to cream, abundantly porphyritic muscovite-biotite granite; euhedral phenocrysts of muscovite and K-feldspar.||||||27-JAN-09
28034|Wongu Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
24583|Wonnemarra Rhyolite|23291|4|Described|p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Croydon Volcanic Group. Thickness: 450-800m. Geological Province: Georgetown Region.||||||08-JUL-15
24583|Wonnemarra Rhyolite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Volcanic No. V801. S-Type.||||||
24583|Wonnemarra Rhyolite|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24583|Wonnemarra Rhyolite|40659|2|Defined|p253|Mesoproterozoic|Mesoproterozoic|||||||
24583|Wonnemarra Rhyolite|40954|6|Mentioned|p132|||||||||
24583|Wonnemarra Rhyolite|41975|6|Mentioned|Fig.3 P433|||||||||
24583|Wonnemarra Rhyolite|43259|4|Described|Appendix 1,p15.||Proterozoic|of Croydon Volcanic Group. Age Middle Proterozoic.||||||
24583|Wonnemarra Rhyolite|43664|6|Mentioned|Fig.3,p15||Mesoproterozoic|||||||
24583|Wonnemarra Rhyolite|50537|6|Mentioned|p3.3|||Of the Croydon Volcanic Group.||||||
24583|Wonnemarra Rhyolite|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Croydon Volcanic Group.  Rhyolitic ignimbrite.||||||
24583|Wonnemarra Rhyolite|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Is overlain conformably by B-Creek Rhyolite.|Bluish-grey moderately crystal-rich rhyolitic ignimbrite with 1-3 mm crystals including rare biotite, garnet and fayalite; 1-5 mm graphite pellets; eutaxitic texture in places.|
24583|Wonnemarra Rhyolite|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Croydon Province.||Unit in Croydon Volcanic Group.||Is overlain conformably by B-Creek Rhyolite.|Bluish-grey moderately crystal-rich rhyolitic ignimbrite with 1-3 mm crystals including rare biotite, garnet and fayalite; 1-5 mm graphite pellets; eutaxitic texture in places.|
24583|Wonnemarra Rhyolite|69591|5|Briefly described|p74 Tb.2.5|||Croydon Province, Georgetown Inlier. 450-800m thick.||Croydon Volcanic Group.|||Crystal-rich rhyolitic ignimbrite.|
23243|Wonomo Granite|50536|5|Briefly described|p1.5, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of hte Sybella Suite.||||||07-NOV-08
23243|Wonomo Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event||Sybella Suite.|||Composite pluton with a strongly foliated to gneissic older phase in the south and younger biotite granite in the north.|
23243|Wonomo Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Composite pluton with a strongly foliated to gneissic older phase in the south and younger biotite granite in the north.|
68211|Woodgate Siltstone|60281|5|Briefly described|Fig. 33 Appendix 1|||Of the Maryborough Formation.  Geological Province: Maryborough Basin.||||||
36245|Woodleigh Granodiorite|23503|5|Briefly described|Map Legend||Late Carboniferous|of Almaden Supersuite.||||||
38187|Woodstock Suite|23422|5|Briefly described|p184, p219 table 6.12|Late Permian|Early Permian|Of Woodstock Supersuite.||||||
38187|Woodstock Suite|69593|4|Described|p494|Permian|Permian|Townsville region: Lolworth Batholith and Charters Towers Province.|~285-265 Ma (Rienks, 1997).|Woodstock Supersuite.|Mount Storth, Castle Hill, Magnetic Island Granites; Mount Stuart Igneous Complex.||Biotite granite; minor diorite, quartz monzodiorite, gabbro.|
38186|Woodstock Supersuite|23422|4|Described|p184, p219 table 6.12|Late Permian|Early Permian|||||||
38186|Woodstock Supersuite|63154|5|Briefly described|p285 Fig. 5|Permian|Permian|Geological province: Charters Towers Province.||||||
38186|Woodstock Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Brodies Camp and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
38186|Woodstock Supersuite|69593|5|Briefly described|p491-494, p496, p504|Permian|Late Carboniferous|Rienks (1997). Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area. I-type, with marginal A-type characteristics.|||Woodstock, Mundic Suites.||Mostly relatively felsic: biotite and hornblende-biotite granodiorite, granite and microgranite as well as hypabyssal equivalents (dacite and rhyolite).|
32157|Woolein Formation|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pl].  Cleaved sandstone, mudstone and subordinate quartz-poor volcaniclastic sandstone.||||||
32157|Woolein Formation|50215|5|Briefly described|Map Legend|Early Permian|Early Permian|Cleaved siltstone, mudstone and subordinate quartz-poor volcaniclastic sandstone.||||||18-JUN-09
32157|Woolein Formation|50317|5|Briefly described|Map Legend|Permian|Permian|Cleaved siltstone, mudstone and subordinate volcaniclastic sandstone.||||||09-JUN-04
32157|Woolein Formation|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Siltstone, mudstone, volcaniclastic sandstone and conglomerate.||||||
32157|Woolein Formation|60282|6|Mentioned|p7|||Supersedes the Woolein beds. Geological Province: Bowen Basn.||||||
32157|Woolein Formation|65388|3|Fully described|p32-34, 11, 34; 31, 43, 48, 146, 163|Early Permian|Early Permian|Connors Arch. After Dear and others (1971) - Rannes beds, Withnall and others (1998a) - "Woolein beds". Lacustrine. Overlies Camboon Volcanics, or may interfinger, although this could be thrust slices. Overlain by Back Creek Group. Correlates: Carmila beds, Goodedulla beds. Consists of khaki-weathering, cleaved siltstone and fine-grained sandstone, superficially similar to cleaved sedimentary rocks of the Back Creek Group. See also p166, 447.||||||
32157|Woolein Formation|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince.||||||
32157|Woolein Formation|68679|5|Briefly described|p312-313, p344, p352, p355, p360|Permian|Permian|Withnall et al. (2009). Auburn Arch, northern New England Orogen. Lacustrine deposits; part of an early Permian rift succession.||||Overlies the Camboon Volcanics. May correlate with the Carmila and Goodedulla beds.|Mainly cleaved siltstone and fine lithofeldspathic sandstone, with coarse-grained  pebbly beds locally. Sourced from the Camboon Volcanics (same radiometric signature).|
36398|Woolooga Granodiorite|23608|3|Fully described|p53-54||Triassic|Revised - now incorporates the southern part of the Green Rock Quartz Monzonite. Also see Fig 1 p 50 + p49 Fig 2 p51. Ar/Ar biotite 234 Ma. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36398|Woolooga Granodiorite|23609|4|Described|p11-12|||Replaces Woolooga Quartz Monzonite to reflect the rock type. 57-67% SiO2. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36398|Woolooga Granodiorite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
36398|Woolooga Granodiorite|68679|5|Briefly described|p411|||See also reference to Woolooga Quartz Monzonite on the same page.||||Contact with Gibraltar Quartz Monzodiorite is a net-vein complex.||
26233|Woolshed Mountain Granodiorite|23799|3|Fully described|p66, p14  Tb. 1|Permian|Permian|Age: 258+/-8Ma (K/Ar, Day et al, 1983).  Unconformably overlain by Main Range Volcanics.  Intrudes Sugarloaf Metamorphics; intruded by Djuan Tonalite.  Geological Province: Yarraman Subprovince (Wandilla Province).  See also p115 Fig. 10.||||||
26233|Woolshed Mountain Granodiorite|23800|5|Briefly described|Map legend|Permian|Permian|||||||
26233|Woolshed Mountain Granodiorite|24560|5|Briefly described|Map legend|Permian|Permian|Light grey, medium-grained granodiorite.||||||
26233|Woolshed Mountain Granodiorite|30303|2|Defined|p322|Late Permian|Middle Permian|Middle to Late Permian age. K/Ar dating 253 m.y.||||||
26233|Woolshed Mountain Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
26233|Woolshed Mountain Granodiorite|35101|4|Described|p69|||||||||
26233|Woolshed Mountain Granodiorite|35161|6|Mentioned|p591|||||||||
26233|Woolshed Mountain Granodiorite|36954|6|Mentioned|p114|||||||||
26233|Woolshed Mountain Granodiorite|37252|6|Mentioned|Map legend|Permian|Permian|||||||
26233|Woolshed Mountain Granodiorite|39445|5|Briefly described|Table 12|||||||||
26233|Woolshed Mountain Granodiorite|42525|5|Briefly described|Map legend|Late Permian|Late Permian|||||||
26233|Woolshed Mountain Granodiorite|43008|5|Briefly described|map legend|||||||||
26233|Woolshed Mountain Granodiorite|60077|5|Briefly described|Map legend|Late Permian|Late Permian|Coarse-grained, equigranular, hornblende-biotite granodiorite.||||||
26233|Woolshed Mountain Granodiorite|60370|5|Briefly described|Map Legend|Permian|Permian|Light grey medium grained granodiorite.||||||
26233|Woolshed Mountain Granodiorite|68679|5|Briefly described|p323, p413-416|Permian|Permian|West of the Esk Basin, northern New England Orogen. Has lower Na2O and K2O and higher CaO. Geochemical plot.|258.2 +/- 8 Ma (K-Ar: Cranfield et al., 1976).|||Intrudes Sugarloaf Metamorphics. Adjacent to Djuan Tonalite.|Grey, medium to coarse granodiorite.|
32150|Woolton Granite Complex|23037|6|Mentioned|p75,6|Permian|Carboniferous|||||||
32150|Woolton Granite Complex|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[CPgwo].  Grey to pink, medium-grained hornblende-biotite granite; greenish grey, medium-grained hornblende-biotite granodiorite.||||||
32150|Woolton Granite Complex|50273|5|Briefly described|Map legend|Early Permian|Late Carboniferous|||||||
32150|Woolton Granite Complex|65388|2|Defined|p279, p236 Fig. 81, p237, 238|Early Permian|Late Carboniferous|Appears to intrude the Torsdale Volcanics. Age tentative.  Includes greenish-grey, medium-grained hornblende-biotite granodiorite to diorite, pinkish-grey medium-grained hornblende-biotite granite and pinkish-orange fractionated leucogranite.||||||
32150|Woolton Granite Complex|68679|5|Briefly described|p404, p408|Permian|Late Carboniferous|Auburn Subprovince, New England Orogen. Lithologies are described in more detail in the text.||||Intrudes Torsdale Volcanics.|Grey, medium-grained biotite-hornblende quartz monzonite with common mafic xenoliths; greenish-grey, medium-grained hornblende-biotite quartz diorite to granodiorite mingled with altered biotite granodiorite; pink fine to medium biotite leucogranite.|
36399|Woonga Granodiorite|23608|3|Fully described|p53||Triassic|Replaces Woonga Quartz Monzonite. Also see p49 Fig 2, p51 and p50 Fig 1. Ar/Ar biotite: 237 Ma. Thermal overprinting by Mount Mucki Diorite. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36399|Woonga Granodiorite|23609|4|Described|p11-12|||Replaces Woonga Quartz Monzonite to reflect the rock type. Of Station Creek Igneous Complex. North D'Aguilar Block.||||||
36399|Woonga Granodiorite|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
36399|Woonga Granodiorite|68679|5|Briefly described|p411|Late Triassic|Late Triassic|Southern part of the northern New England Orogen. ~36 km2. Regional magnetic images show circular, concentrically zoned body ~8km in diameter.|237 +/- 0.5 Ma (Ar-Ar biotite: Tang 2004).|Station Creek Igneous Complex.|||(Hornblende-)biotite quartz monzonite. Cryptic outcrop; normal zonation from granodiorite-tonalite rim to granodiorite centre.|
23257|Woongalee Granodiorite|23032|5|Briefly described|p39|||||||||
23257|Woongalee Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
23257|Woongalee Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
23257|Woongalee Granodiorite|43480|2|Defined|7-39|Devonian|Silurian|Age: 407Ma||||||
23257|Woongalee Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Moderately to strongly foliated, grey to dark grey, (sphene-)epidote-biotite and sphene-epidote-hornblende-biotite granodiorite and tonalite.||||||
23257|Woongalee Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Moderately to strongly foliated, grey to dark grey, (sphene-)epidote-biotite and sphene-epidote-hornblende-biotite granodiorite and tonalite.|
23257|Woongalee Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Moderately to strongly foliated, grey to dark grey, (sphene)-epidote-biotite and sphene-epidote-hornblende-biotite granodiorite and tonalite.|
23257|Woongalee Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Moderately to strongly foliated, grey to dark grey, (sphene)-epidote-biotite and sphene-epidote-hornblende-biotite granodiorite and tonalite.|
23257|Woongalee Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.|410 +/- 6 Ma (SHRIMP U-Pb zircon).|Upland Supersuite.|||I-type.|
27306|Woonigan Granite|24197|5|Briefly described|p21, p94 Tb. 1.1|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite.Age: 1860Ma. Geological province: Mount Isa Inlier.||||||07-FEB-11
27306|Woonigan Granite|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27306|Woonigan Granite|37862|4|Described|p584|||||||||
27306|Woonigan Granite|38350|4|Described|p16|||||||||
27306|Woonigan Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27306|Woonigan Granite|38658|6|Mentioned|p153|||||||||
27306|Woonigan Granite|38900|6|Mentioned|p55|||||||||
27306|Woonigan Granite|39445|5|Briefly described|Table 2|||||||||
27306|Woonigan Granite|40840|6|Mentioned|Map legend|||||||||
27306|Woonigan Granite|45161|4|Described|p29|||||||||
27306|Woonigan Granite|45166|5|Briefly described|p33|||||||||
27306|Woonigan Granite|49009|2|Defined|p50|Proterozoic|Proterozoic|Previously mapped as Kalkadoon Gr. & Leichhardt Met.(Carter & Opik,1963)||||||
27306|Woonigan Granite|49041|5|Briefly described|Table 2|||||||||
27306|Woonigan Granite|50536|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
27306|Woonigan Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Fine to coarse leucocratic biotite granite.||||||
27306|Woonigan Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event||Kalkadoon Supersuite.|||Leucocratic biotite granite|
27306|Woonigan Granite|69591|6|Mentioned|p60|||Wonga Batholith.|||||Leucocratic biotite granite.|
27306|Woonigan Granite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Equivalent to Kalkadoon Granodiorite, Mayfield Gneiss, Plum Mountain Gneiss.|Leucocratic biotite granite.|
27306|Woonigan Granite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain.||||Shown as probably older than Magna Lynn Metabasalt and younger than Leichhardt Volcanics. Equivalent to Kalkadoon Granodiorite, Mayfield Gneiss, Plum Mountain Gneiss.|Leucocratic biotite granite.|
33431|Wooroolin Granite|23799|3|Fully described|p73, p13 Tb. 1|Triassic|Permian|Previously mapped as part of Boondooma Ig. Complex (Murphy et al, 1976).  Age: 274+/-28Ma (Rb/Sr), 258.2Ma (K/Ar) and 258.2Ma (Webb et al, 1965).  Intrudes Maronghi Cr. beds and Fifer Creek Metamorphics.  f the South-east Qld. Volc. and Plut. Intrusives.||||||
33431|Wooroolin Granite|23800|5|Briefly described|Map Legend|Late Triassic|Permian|||||||
33431|Wooroolin Granite|50384|5|Briefly described|Map Legend|Triassic|Late Permian|||||||
33431|Wooroolin Granite|60371|5|Briefly described|Map Legend|Triassic|Permian|Medium-grained biotite leucogranite; intruded by scattered aplite dykes.||||||03-SEP-04
33431|Wooroolin Granite|68679|5|Briefly described|p415||||258.2 Ma K-Ar: Webb abd McDougall (1968).||||Dominantly granitic; ranges to gabbro and diorite; unfoliated.|
37119|Wooroonden Granodiorite|23799|4|Described|p96, p11 Tb. 1|Triassic|Triassic|Previously mapped as part of Wigton Adamellite (Murphy et al, 1976).  Biotite-hornblende granodiorite.  Unconformably overlain by Oakdale Sandstone.  Probably intrudes Aranbanga Group.  Geological Province: Yarraman Subprovince (Wandilla Province).||||||23-NOV-05
37119|Wooroonden Granodiorite|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
37119|Wooroonden Granodiorite|68679|5|Briefly described|p415, p428-429|Late Triassic|Late Triassic|Northern New England Orogen. Hosts minor gold mineralisation; has been explored for epithermal and porphyry style deposits.|||||Variable: dominantly a fine- to medium-grained, equigranular biotite-hornblende granodiorite; a zoned pluton was suggested, ranging gradationally from marginal gabbro through diorite, quartz diorite and granodiorite, to a granite centre.|
80782|Woowoonga Range Monzogranite|68679|5|Briefly described|p420-421, p430|Late Triassic|Late Triassic|Gayndah-Gladstone belt. A small, arcuate pluton.||||Adjacent to Broomfield Granite.|Biotite monzogranite.|
23261|Worcester Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|||||||
23261|Worcester Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 275. I-Type.||||||
23261|Worcester Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Pale grey, medium-grained hornblende-biotite granite.||||||15-JUN-06
23261|Worcester Granodiorite|43259|4|Described|Appendix 1,p35.||Late Carboniferous|||||||
23261|Worcester Granodiorite|60425|4|Described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Two subunits probably representing discreet plutons: (1) pale grey, med.-grained, hornblende-biotite granite, and (2) pale-med.grey, med.-grained, slightly porphyritic two pyroxene-hornblende-biotite granodiorite to granite. I-type. See also Worc.Granite||||||07-FEB-11
24125|Worthington Formation|24420|5|Briefly described|p9|Eocene|Eocene|Of The Narrows Group.||||||
24125|Worthington Formation|24490|5|Briefly described|Map Legend|Tertiary|Tertiary|Sandstone, siltstone, claystone, conglomerate.  In the Narrows Graben.||||||01-JUL-14
24125|Worthington Formation|37676|3|Fully described|p7|||||||||
24125|Worthington Formation|38658|6|Mentioned|p152|||||||||
24125|Worthington Formation|39943|6|Mentioned|Table 13A|||||||||
24125|Worthington Formation|40116|4|Described|p28|||||||||
24125|Worthington Formation|41927|4|Described|p68|||||||||
24125|Worthington Formation|42021|6|Mentioned|Fig.3 P320|||||||||
24125|Worthington Formation|50207|5|Briefly described|Map Legend|Tertiary|Tertiary|Of the The Narrows Group.||||||
24125|Worthington Formation|71092|5|Briefly described|p232-233|Eocene|Eocene|The Narrows Graben, SE Queensland.||||Is overlain by Rundle Formation.||
23263|Wotan Granodiorite|23423|6|Mentioned|p240|||||||||
23263|Wotan Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 303.  I-Type.||||||
23263|Wotan Granodiorite|23713|5|Briefly described|p75 Appendix 2|||Intrudes Kitoba Member. Overlain by Nychum Volcanics - unconformable.||||||01-JUN-09
23263|Wotan Granodiorite|43083|4|Described|p253|||Of the Almaden Supersuite.I-type.  Lithology included.||||||17-JUN-09
23263|Wotan Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite  (Almaden Supersuite).||||||15-JUN-06
23263|Wotan Granodiorite|43254|5|Briefly described|map legend||Late Carboniferous|Of the Almaden Supersuite.||||||01-JUN-09
23263|Wotan Granodiorite|43259|4|Described|Appendix 1,p37.||Late Carboniferous|||||||
23263|Wotan Granodiorite|43625|6|Mentioned|p49|||||||||
23263|Wotan Granodiorite|60425|4|Described|p45 Tb. 3, p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Unconformably overlain by Nychum Volcanics.Grey to pale pink (altered), fine-grained, moderately to highly porphyritic hornblende-biotite granodiorite; mafic enclaves to 15cm common. I-type.||||||07-FEB-11
36787|Wratten Igneous Suite|23608|5|Briefly described|p50 Fig.1||Carboniferous|See also page 51 fig.3.  Transitional S- to I-type granite. Geol. Province: North D'Aguilar Block.||||||
36787|Wratten Igneous Suite|68679|5|Briefly described|p403, p405|Permian|Carboniferous|Tang and Gust (2000). A transitional S-type to I-type Suite. Interpreted as syn-tectonic and forming a sill-like structure.|||Claddagh, Gallangowan, Karandah Granodiorites.||Calc-alkaline, peraluminous granodiorites; weakly foliated; localised cataclastite and recrystallised lamellae; leucocratic, brittle-deformed, biotite-hornblende granodiorite to granite. Supracrustal metasedimentary source.|
36505|Wulguru granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 149.||||||
28012|Wulpan Monzogranite|23420|5|Briefly described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intrudes Holroyd Group.||||||
28012|Wulpan Monzogranite|43596|4|Described|p25, p26 Tb. 2, p29 Tb. 3|||Of Flyspeck Supersuite. Intrudes Sugarbag Creek Quartzite. Medium to dark grey equigranular biotite monzogranite.||||||15-JAN-09
28012|Wulpan Monzogranite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
41942|Wundaru Granodiorite|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Light grey, fine- to medium-grained, equigranular biotite hornblende granodiorite.||||||
41942|Wundaru Granodiorite|65388|2|Defined|p418-419, p415, p403 Fig. 135, p410, 420|Early Cretaceous|Early Cretaceous|Intrudes Carmila beds. Intruded by unnamed ?Tertiary dykes. K-Ar dating of biotite and hornblende gave same age: 130+/-1 Ma, suggesting this is near crystallisation age. Very poorly exposed. Moderately altered to fresh, light grey, fine to medium-grained, equigranular titanite-biotite-hornblende granodiorite can be found as boulder-sized kernels.||||||
36243|Wurruma Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite?.||||||
36243|Wurruma Granite|60425|4|Described|p280-1 Appdx.|Late Carboniferous|Late Carboniferous|Possibly part of Ootann Supersuite? I-type. Porphyritic biotite granite; previously informally referred to as Airport granite porphyry.||||||07-FEB-11
33452|Wyalla Granite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgaw].  Pink, medium-grained biotite granite.||||||
33452|Wyalla Granite|50197|5|Briefly described|Map Legend|Triassic|Permian|Of the Galloway Plains Igneous Complex.||||||
33452|Wyalla Granite|68008|2|Defined|p350, p372, p381, p386-387|Early Triassic|Permian|New name, from the property Wyalla. Located just S of the Dawson Highway, 40km NE of Biloela. A small pluton, 2 x 1km. The type area is along a track to a powerline pylon 1.5km SE of Wyalla homestead. Forms steep hills. Geophysics described: distinguished from Dumgree Tonalite and Rocky Point Granodiorite. Geochemistry described. No age determination.||Galloway Plains Igneous Complex.||Intrudes Rocky Point Granodiorite.|Pale pink, massive, medium-grained biotite granite.|
33452|Wyalla Granite|68679|4|Described|p424-425, p427|||Yarrol Province. Forms a 2 x 1 km intrusion. Geochemistry briefly described.|~251 Ma.|Galloway Plains Igneous Complex.||Is intruded by Rocky Point Granodiorite.|Biotite granite.|
24588|Wyandotte Formation|42580|4|Described|p285|Pleistocene|Pleistocene|||||||
24588|Wyandotte Formation|42587|5|Briefly described|p107|||Check Spelling in reference.||||||
24588|Wyandotte Formation|69600|5|Briefly described|p660|Pleistocene|Pleistocene|Wyandotte Creek, SW of Cairns. Contains eleven discrete Pleistocene fossil fauna-bearing units.|||||Indurated gravels, sands and clays.|
24588|Wyandotte Formation|69789|6|Mentioned|p1042|Quaternary|Quaternary|Wyandotte Creek near Greenvale. Late Quaternary fluvial and/or lacustrine deposits. Contains vertebrate remains.||||||
24588|Wyandotte Formation|73115|6|Mentioned|p25, p29|Pleistocene|Pleistocene|McBride Basalt Province. Fossiliferous. One of few described instances of sedimentary interbedding in the province.||||Underlain by Masterson Basalt.||
80221|Wyarra Granite|70740|5|Briefly described|p102, p130|||Outcrop characteristics and geophysical characteristics briefly discussed. ||||Intrudes the Bulgonunna Volcanic Group.|Fine-grained, porphyritic leucogranite, light-grey, medium-grained porphyritic hornblende-biotite tonalite.|
80221|Wyarra Granite|73035|5|Briefly described|Map legend|Early Permian|Late Carboniferous||||||Pale brown to cream, fine-grained, porphyritic leucogranite; light grey, medium-grained porphyritic hornblende-biotite tonalite.|
74881|Wycarbah Volcanics|68008|2|Defined|p225, p246-251, p254, p261, p264, p493|Early Cretaceous|Early Cretaceous|See also p530-531, p565. Wycarbah area, c.35km WSW of Rockhampton. Forms Mount Hay. The type area is given as that section of rocks exposed between the Wycarbah and Mount Hay plugs, with numerous exceptions (listed): see Kay (1981). Geochemistry detailed; similarities with Mount Hedlow Trachyte. Also resembles Mount Salmon Volcanics but is more rhyolitic. Radiometric response indistinguishable from Bushley Dacite. Estimated thickness 110m. Contains plant fossils. Several U-Pb zircon ages given; Rb-Sr and U-Pb data tabulated. Hosts numerous mining leases for gemstone and lapidary materials (thunder eggs, agate, amethyst).|c.129-c.109 Ma.|||Is overlain possibly conformably by Dalma Basalt.|Rhyolite and trachyte plugs accompanied by rhyolite and trachyte flows and pyroclastic deposits (all described in detail).|
74881|Wycarbah Volcanics|69594|5|Briefly described|p551-552, p559-560, p563|Cretaceous|Cretaceous|Stanwell Basin. Occurs from Mount Hay near Wycarbah to ~14km NW. Largely non-marine; tree trunks in growth position reported. Plugs form steep-sided domes; lavas form flat-topped ridges. Several age determinations given.|120.2 +/- 0.3 Ma (U-Pb TIMS).|||Is overlain by Dalma Basalt.|Rhyolitic and trachytic to monzonitic plugs, trachyte, rhyolite, spherulitic rhyolite ignimbrite, breccia; numerous tree stumps. Elaborated on p560.|
74881|Wycarbah Volcanics|73450|4|Described|p4, p51-52, p54|early Cretaceous|early Cretaceous|Forms eroded domes and flat-topped ridges in the vicinity of and NW of Wycarbah township, and two smaller bodies further south. Constitutes numerous rhyolite and trachyte plugs, flows and pyroclastic deposits. Plugs are mapped as a separate subunit (Kvw/i). Rhyolite is locally spherulitic with sporadic development of 'thunder eggs' and agatised rhyolite. Some pyroclastic deposits contain (early Cretaceous) plant fossils including in-situ tree stumps. Yielded a range of U-Pb TIMS zircon ages including 128.0 +/- 0.4 Ma (soil profile), 120.2 +/- 0.3 Ma and 108.5 +/- 0.3 Ma (colourless and amber zircon, respectively, from the same pyroclastic deposit), and 237.8 +/- 0.7 Ma (intrusion; explained as xenocrystic) (Murray et al., 2012). Probably part of the same episode of within-plate volcanism as the Dalma Basalt. May be difficult to distinguish from the Mount Salmon Volcanics.||||Overlain by Dalma Basalt.|Fine- to coarse-grained, brecciated, and flow banded rhyolite, fine- to medium-grained trachytic, and pyroclastic deposits ranging from coarse breccias to fine-ash tuffs.|
80222|Wynne Creek Diorite|70740|5|Briefly described|p29, p49, p120, p130|Permian|Carboniferous|Previously the Percy Douglas Granodiorite. Outcrop characteristics briefly discussed.||||Intrudes the Ukalunda Formation, Les Jumelles Beds and Mount Wyatt Formation.|Grey, fine to medium-grained, clinopyroxene-hornblende quartz diorite.|05-OCT-17
69183|Yaamba beds|60557|5|Briefly described|p19 Fig. 5b, p28|Tertiary|Tertiary|||||||
69183|Yaamba beds|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||
69183|Yaamba beds|67402|4|Described|p239, p262, p263|Aldingan|Johannian|Yaamba Basin. Unsuitable reservoir for the storage of carbon dioxide. Lacustrine to paludal and fluvio-lacustrine depositonal environments. Up to 750m thick. |||||Mudstone, shale, oil shale, sandstone and lignite.|
69183|Yaamba beds|68008|4|Described|p275-277|Eocene|Eocene|Exploration revealed a Tertiary basin near Yaamba (Olive et al., 1984). The Basin fill was named Yaamba Group (Willmott et al., 1986), but in the absence of consituents being defined, is here renamed Yaamba beds. Estimated 900m thick; possibly 1300m. Middle to late Eocene age from microflora.|||||Brown oil shale, green shale and mudstone; carbonaceous and lignitic oil shale, carbonaceous mudstone and shale, green mudstone and sandstone; quartz sandstone, sandy mudstone (SSW) or basaltic conglomerate, pebbly mudstone, lithic sandstone (NNE).|
69183|Yaamba beds|69599|5|Briefly described|p586, p589|Eocene|Eocene|Yaamba Basin. Up to 750m thick. Mainly lacustrine deposits with associated fluvial inputs. No economic oil shale resources discovered. RELATED UNITS (continued): Also correlated (at least partly) with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Water Park Creek, Herbert Creek and Rossmoya beds; Flinders Dolomite; see COMMENTS for more.|Oil shale, claystone, siltstone and carbonaceous shale, grading outwards to sandstone and conglomerate approaching the Basin margins.|
29746|Yabba Creek Granodiorite|22845|6|Mentioned|Fig6||Carboniferous|||||||
29746|Yabba Creek Granodiorite|22846|4|Described|p6,10,20,plate1|Stephanian|Namurian|Part of the Capsize Creek Complex||||||
29746|Yabba Creek Granodiorite|23608|4|Described|p50 Fig 1, p51 Fig 3.||Carboniferous|311 Ma. Also see p51. I-type intrusion.||||||
29746|Yabba Creek Granodiorite|43588|6|Mentioned|p30||Late Carboniferous|||||||
29746|Yabba Creek Granodiorite|60370|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Geological Province: North D'Aguilar Subprovince. Massive to slightly foliated hornblende-biotite granodiorite.||||||02-SEP-04
29746|Yabba Creek Granodiorite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|North D'Aguilar Subprovince. This unit, as well as the Capsize Creek Complex; the Coppermine Creek, Gallangowan, Karandah and Claddagh Granodiorites, are all mapped under the same symbol, Cgd.||||||
29746|Yabba Creek Granodiorite|68679|5|Briefly described|p403, p405|Permian|Carboniferous|North D'Aguilar Subprovince. A unit in an un-named group of foliated diorite-granodiorite intrusions.|310 +/- 0.6 Ma (maximum cooling age).||||Medium-grained, massive to slightly foliated hornblende-biotite granodiorite.|
79368|Yacamunda Creek Dacite|70740|3|Fully described|i, iv, p83, p95-p96, p98-p99, p116|||Drummond Basin. In previous work this ignimbrite was mapped either as coherent rhyolite, Bobby Dazzler Rhyolite or as unnamed Drummond Basin ignimbrite unit. Appears to be a single ignimbrite sheet. Outcrop characteristics and distribution discussed. Lithology and petrography are discussed in detail. Named for the Yacamunda Creek which is a tributary of Black Creek. Up to 80m thick.  A type locality is nominated and only very briefly described.||Bulgonunna Volcanic Group||Probably overlies the Bimurra Volcanics, Bungobine Rhyolite.|Relatively homogenous, lithic to crystal-rich, strongly welded dacitic ignimbrite.|
79368|Yacamunda Creek Dacite|73035|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous||||||Light brown-slightly purplish, crystal to lithic-rich, strongly welded dacitic ignimbite; abundant fragments of plagioclase, alkali feldspar, some biotite and possibly hornblende, very minor quartz; common fragments of coherent felsic lava.|
29182|Yam Creek beds|24393|5|Briefly described|p152|Miocene|Miocene|Fluvial sediments displaying increasing clast size and bed thickness in the downstream direction.  Geological Province: Carpentaria Basin.||||||
29182|Yam Creek beds|42550|4|Described|p9|||Variation on old Yam Creek Beds.||||||
29182|Yam Creek beds|42637|6|Mentioned|p31|||||||||
29182|Yam Creek beds|49769|6|Mentioned|p4|||||||||
29182|Yam Creek beds|61155|5|Briefly described|p20|Late Miocene|Middle Miocene|Thickness together with Lilyvale beds: 65m. In eastern Cape York.||||||
29182|Yam Creek beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as the Falloch, Lilyvale and Wyaaba beds, are all mapped under the symbol, Tu.||||||
29182|Yam Creek beds|69599|5|Briefly described|p580, p585, p602-603|Pliocene|Miocene|Karumba Basin, Carpentaria region. Crops out near Cape Weymouth. Up to 65m thick. Fluvial to possibly lacustrine. Silcrete weathered surface.||||Correlated with Lilyvale, Wyaaba and Falloch beds and ?Campaspe Formation.|Clayey quartzose sandstone, granule and pebbly conglomerate and interbedded sandy claystone.|
29182|Yam Creek beds|70207|6|Mentioned|p126|||Tertiary.||||||
29182|Yam Creek beds|71792|5|Briefly described|p2, p9, p59-p62|Pliocene|Miocene||||||Fluviatile clayey quartzose sandstone and granule conglomerate, locally pebbly; interbedded sandy claystone; lateritised.|
29182|Yam Creek beds|71853|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartzose sandstone and granule conglomerate, locally pebbly; interbedded sandy claystone; fluviatile deposits, lateritised.|
29182|Yam Creek beds|72983|6|Mentioned|p110|Miocene|Miocene|||||||
23282|Yambo Metamorphic Group|22781|6|Mentioned|p11|||||||||
23282|Yambo Metamorphic Group|22811|5|Briefly described|p597, Fig.3 p599|Mesoproterozoic|Paleoproterozoic|of Yambo Subprovince||||||07-NOV-08
23282|Yambo Metamorphic Group|23291|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Deposited between 1640-1580 Ma. Geological Province: Yambo Inlier.||||||08-JUL-15
23282|Yambo Metamorphic Group|23420|4|Described|p 144 table 4.4||Paleoproterozoic|Also see p 118- 119. In the Yambo Subprovince. Probably younger than ~1643Ma (detrital zircons).  Previously Dargalong Metamorphics.||||||07-NOV-08
23282|Yambo Metamorphic Group|23422|5|Briefly described|Plate 7.3|Proterozoic|Proterozoic|||||||
23282|Yambo Metamorphic Group|23423|5|Briefly described|p300 Table 7.2|||||||||
23282|Yambo Metamorphic Group|23430|5|Briefly described|p451|||||||||
23282|Yambo Metamorphic Group|23496|5|Briefly described|Table 1||Proterozoic|||||||
23282|Yambo Metamorphic Group|23713|4|Described|p10-11|Early Devonian|Late Silurian|Previously described as part of the Dargalong Metamorphics. Includes Chelmsford Gneiss. Yambo Province.||||||
23282|Yambo Metamorphic Group|24485|5|Briefly described|p1, 21|Mesoproterozoic|Paleoproterozoic|Correlated with the Dargalong Metamorphics. Age: ~1643-1580Ma||||||20-MAR-13
23282|Yambo Metamorphic Group|43254|5|Briefly described|map legend||Mesoproterozoic|||||||
23282|Yambo Metamorphic Group|43285|5|Briefly described|Map Legend|||age Middle Proterozoic.||||||
23282|Yambo Metamorphic Group|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
23282|Yambo Metamorphic Group|43596|4|Described|p6, p8, p20 Tb.1||Proterozoic|Previously described in detail by Trail et al (1968) as the Dargalong Metamorphics. Part of Yambo Province, together with Newberry Metamorphic Group.||||||15-JAN-09
23282|Yambo Metamorphic Group|43625|14|Not recorded|p15,Table 1|||||||||
23282|Yambo Metamorphic Group|43665|4|Described|p11||Proterozoic|||||||
23282|Yambo Metamorphic Group|43820|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23282|Yambo Metamorphic Group|50537|6|Mentioned|p6.1|||Geological Province: Yambo Inlier.||||||
23282|Yambo Metamorphic Group|60357|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Includes: Kokojelandji Schist, Chelmsford Gneiss. Geological Province: Yambo Subprovince.||||||07-NOV-08
23282|Yambo Metamorphic Group|60358|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Includes: Kokojelandji Schist, Chelmsford Gneiss. Geological Province: Yambo Subprovince.||||||07-NOV-08
23282|Yambo Metamorphic Group|60425|6|Mentioned|p15 Tb. 1, p29|||Little River C. M. are faulted against these rocks. These rocks enclose a fault-bounded lens of undivided Hodgkinson Province rocks west of Palmerville Fault.||||||07-FEB-11
23282|Yambo Metamorphic Group|63866|4|Described|p76, p79-p80, p85|Calymmian|Calymmian|Yambo Subprovince, Coen Region. Crops out in the southern part of the Coen Region. Faulted against the Hodgkinson Province. Divided into thirteen metamorphic units (not all named here). Numeric age provided is interpreted as the igneous crystallisation age of the mafic precursor to a granulite from this group.|1586 +/- 4 Ma (Blewett et al., 1998)||Includes the Arkara Gneiss.||High-grade metasedimentary and meta-igneous rocks.|
23282|Yambo Metamorphic Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||||||
23282|Yambo Metamorphic Group|69591|4|Described|p61, p70-73, p76-77, p79|Paleoproterozoic|Paleoproterozoic|Blewett and Wilford (1996). Yambo Inlier, Yambo Subprovince, Etheridge Province. Previously included in the Dargalong Metamorphics. Crops out over 1500 km2. Underwent six regional deformation events (described). See also references to Yambo Metamorphics (p70).|1640-1580 Ma (Blewett et al., 1998).||Daintree, Chelmsford, Arkara, Pombete Gneisses; Twelve Mile, Kokojelandji, Jedda, Saraga, Annie Creek, Oswald Schists.||High-grade metasedimentary and meta-igneous rocks including schist, quartzite, orthogneiss, paragneiss, amphibolite and mafic granulite.|
23282|Yambo Metamorphic Group|69592|6|Mentioned|p241|Mesoproterozoic|Mesoproterozoic|Coen Inlier. Has detrital ages around 1580-1477 Ma.||||||
23282|Yambo Metamorphic Group|70207|5|Briefly described|p4, p74|Proterozoic|Proterozoic|North Australian Craton.||||Is intruded by Lukinville Granodiorite.||
23282|Yambo Metamorphic Group|70345|6|Mentioned|p3|Mesoproterozoic|Palaeoproterozoic|||||||
23282|Yambo Metamorphic Group|70673|6|Mentioned|p7|||Age range given as Paleoproterozoic-Mesoproterozoic.||||||
23282|Yambo Metamorphic Group|70822|5|Briefly described|p112|Mesoproterozoic|Palaeoproterozoic||~1600 Ma||||Mafic granulites.|
23282|Yambo Metamorphic Group|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1585+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss, 2-pyroxene mafic granulite.|
23282|Yambo Metamorphic Group|71792|6|Mentioned|p3|||||||||
23282|Yambo Metamorphic Group|72983|6|Mentioned|p15|Mesoproterozoic|Paleoproterozoic|||||||
23282|Yambo Metamorphic Group|73083|6|Mentioned|p67, p76|||||||||
24133|Yan Can Greenstone Member|22557|6|Mentioned|p569|||||||||
24133|Yan Can Greenstone Member|42747|5|Briefly described|p32, Fig.3|||of Bathampton Metamorphics||||||
24133|Yan Can Greenstone Member|43204|5|Briefly described|Map Legend|Cambrian|Neoproterozoic|of Bathampton Metamorphics. Neoproterozoic or Early Cambrian. Anakie Inlier.||Bathampton Metamorphics||||23-DEC-11
24133|Yan Can Greenstone Member|43213|2|Defined|p8, p20-21, p25-26, p34, p46-51, p133|||See also p150, p204-205, p235, p240. Named after Yan Can Block, the name given to Portion 13, Parish of Drummond. Main outcrop centred about 25 km WSW of Clermont. Over several hundreds of metres thick. Formally named because of its size and relative homogeneity. Type area described. May have been a pile of basaltic lavas. Geochemistry, geophysics  and chemical analyses detailed. Offset 2.5 km by Grasstree Fault.||Unit in Bathampton Metamorphics.|||Well foliated, green chlorite schist locally enclosing massive to weakly foliated, ellipsoidal pods of fine-grained greenstone several metres long. Minor local quartzite (?metachert), marble and calc-silicate rocks.|
24133|Yan Can Greenstone Member|43861|2|Defined|25; Fig1p26; p28|Late Cambrian|Early Cambrian|In Bathampton Metamorphics.||||||03-APR-08
24133|Yan Can Greenstone Member|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Bathampton Metamorphics.|||Green, fine-grained, foliated greenstone and calcite-chlorite-actinolite-epidote schist; minor fine-grained mica schist and quartzite.|
24133|Yan Can Greenstone Member|68731|5|Briefly described|p120, p124 Tb 3.1|Neoproterozoic|Neoproterozoic|Contains rare igneous textures with randomly oriented plagioclase laths. Strongly foliated with fine layering. Minimum age constrained by the parent Bathampton Metamorphics.||Of the Bathampton Metamorphics.|||Comprises flat-lying mafic schist and minor mica schist, local calc-silicate rocks.|
37055|Yandina Creek Rhyolite|23251|5|Briefly described|Table 1 p8|Late Triassic|Late Triassic|Probably an abbreviation of Yandina Creek Rhyolite Member.||||||21-JUN-06
37055|Yandina Creek Rhyolite|44925|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics||||||
37055|Yandina Creek Rhyolite|44928|5|Briefly described|Map Legend||Late Triassic|Of North Arm Volcanics Group. Pumice and clast-rich rhyolitic ignimbrite; breccia horizon.||||||31-MAY-06
37055|Yandina Creek Rhyolite|68679|5|Briefly described|p437|Late Triassic|Late Triassic|Sunshine Coast hinterland.||North Arm Volcanic Group.||Conformably overlies Kullangor Member.|Crystal-poor rhyolitic ignimbrite; clasts include flattened pumice, andesite and spherulitic rhyolite.|
37055|Yandina Creek Rhyolite|73450|6|Mentioned|p84|Triassic|Triassic|||||||
79960|Yankalilla Gabbro|71965|6|Mentioned|p906|||Geological province: Thomson Orogen. ||||||
40144|Yaparaba Volcanics|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pvp].  Basaltic to dacitic lava and volcaniclastic rocks, rhyolitic ignimbrite and some lithic sandstone and conglomerate.||||||
40144|Yaparaba Volcanics|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
40144|Yaparaba Volcanics|60282|5|Briefly described|p10, p15|Early Permian|Early Permian|On the SCORIA and BANANA map sheets.  Contain marine macrofossils indicating a marine depositional environment. May be a Rookwood Volcanics equivalent?||||||
40144|Yaparaba Volcanics|65388|3|Fully described|p35-39, 36, 37, 26, 32, 338, 435,439,447|Early Permian|Late Devonian|Nogo Subprovince, Yarrol Province. A new unit in central SCORIA. Includes fossils previously reported as in Camboon Volcanics. Partial correlate with Camboon Volcanics. Faulted contact with Back Creek Group and Camboon Volcanics. include aphyric to slightly porphyritic basalt, andesite and dacite and generally poorly sorted, volcaniclastic conglomerate and sandstone; subordinate crystal-rich, lithic-rich rhyolitic or dacitic volcaniclastic rocks, including probable ignimbrite crops out in places.||||||
40144|Yaparaba Volcanics|68008|5|Briefly described|p419, p421|||Previously part of the Rannes beds in the Biloela district.||||Adjacent to (probably intruded by) Lookerbie Igneous Complex.||
40144|Yaparaba Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince. This unit, with the Narayen, Nogo and Smoky beds, are all mapped under the symbol, Pvy.||||||
40144|Yaparaba Volcanics|68679|5|Briefly described|p312-313, p343-344, p352, p416, p419|Late Devonian|Late Devonian|Withnall et al. (2009). SSW of Biloela, Nogo Subprovince, northern New England Orogen. Originally mapped as Camboon Volcanics by Dear et al. (1971); renamed because they are separated by the Grevillea Thrust and Back Creek Group. Part of the Rawbelle Batholith. Relatively undeformed. Age is uncertain; geochemical evidence suggests equivalence with the nearby Lochenbar Formation.||||Is intruded by Wingfield Granite.|Basaltic to dacitic lavas; some outcrops may be dykes. Some volcaniclastics (subaerial debris or mass flows): massive, poorly sorted. Scattered outcrops of well-bedded, volcanilithic sandstone and lesser conglomerate and siltstone.|
37899|Yappar River Dolerite|23291|5|Briefly described|p98 Tb. 3.11, p48,49|Early Permian|Early Permian|Of the Western Georgetown Region. Age: ca.280 Ma. Geological Province: Georgetown Region.||||||08-JUL-15
26242|Yardida Tillite|8187|5|Briefly described|Map legend|Adelaidean|Adelaidean|Diamictite, shale, siltstone, sandstone.  Overlain by Black Stump Arkose.||||||21-JUN-04
26242|Yardida Tillite|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Laminated black shale with dolomite lenses. Underlies: Black Stump Arkose.||||||28-OCT-04
26242|Yardida Tillite|24442|5|Briefly described|p49|Sturtian|Sturtian|Geological Province: Georgina Basin.||||||
26242|Yardida Tillite|35863|6|Mentioned|Table 1|||||||||
26242|Yardida Tillite|36234|6|Mentioned|p164|||||||||
26242|Yardida Tillite|36898|6|Mentioned|p181|||||||||
26242|Yardida Tillite|37462|4|Described|Table 4.IX|||||||||
26242|Yardida Tillite|37928|6|Mentioned|Fig.4|||||||||
26242|Yardida Tillite|37929|4|Described|p525|||||||||
26242|Yardida Tillite|38157|6|Mentioned|Table IX|||||||||
26242|Yardida Tillite|38832|6|Mentioned|p157|||||||||
26242|Yardida Tillite|39445|6|Mentioned|p56|||||||||
26242|Yardida Tillite|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26242|Yardida Tillite|40906|6|Mentioned|Fig.9|||||||||
26242|Yardida Tillite|41277|5|Briefly described|p83|||||||||
26242|Yardida Tillite|41405|6|Mentioned|p205|||||||||
26242|Yardida Tillite|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
26242|Yardida Tillite|44158|6|Mentioned|p29|||In the Georgina Basin.||||||20-DEC-06
26242|Yardida Tillite|45155|6|Mentioned|Fig.7|||In the Georgina Basin.||||||20-DEC-06
26242|Yardida Tillite|46903|6|Mentioned|p53|||||||||
26242|Yardida Tillite|46959|6|Mentioned|p207|||||||||
26242|Yardida Tillite|48990|2|Defined|p16|Adelaidean|Adelaidean|||||||
26242|Yardida Tillite|49027|6|Mentioned|p2|||||||||
26242|Yardida Tillite|60122|4|Described|p9, p11, p41|Neoproterozoic|Neoproterozoic|Green-grey diamictite siltstone, dolomitic shale, dolostone, minor quartz sandstone, arkose. Disconformable on Yacha beds; disconformably overlain by Black Stump Arkose.  Max. thickness: 2900m. Geological Province: Georgina Basin. In Supersequence 2.||||||24-MAY-05
26242|Yardida Tillite|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Diamictite, siltstone, dolomitic shale, dolostone, minor quartz sandstone and arkose.||||||
26242|Yardida Tillite|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Aroota Group.  Diamictite, siltstone, dolomitic shale, dolostone, minor quartz sandstone and arkose. Geological Province: southern Georgina Basin.||||||
26242|Yardida Tillite|62082|6|Mentioned|p66|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
26242|Yardida Tillite|63450|5|Briefly described|p78 Fig. 5|Neoproterozoic|Neoproterozoic|Disconformably overlies Yackah beds; disconformably overlain by Black Stump Arkose and Wonnadinna Dolomite. Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
26242|Yardida Tillite|64068|3|Fully described|p45, 46, p19, p151, p223|Cryogenian||Over 650 m thick.||Of Aroota Group.||Disconformably overlies Yackah beds. Is disconformably overlain by Black Stump Arkose.|Green-grey diamictite and laminated siltstone;  minor fine to coarse quartz sandstone and arkose. Local dolomitic capping.|04-APR-12
26242|Yardida Tillite|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Toko Syncline, Southern Georgina Basin.||||||
26242|Yardida Tillite|65338|6|Mentioned|p63.|||Southeastern Georgina Basin. May correlate with the diamictite at the base of Central Mount Stuart Formation.||Unit in Aroota Group.||||
26242|Yardida Tillite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Tillite.|
26242|Yardida Tillite|68270|4|Described|p681-683,686-688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section is a composite section with outcrop in Field River Anticline and area 6km SSE of Aroota Bore, drillholes Hay River 5 (lat. 23'11'9"N, long. 137'54'12"E) 6 (lat 23'10'42N, long. 137'52'48"E) and section at the end of seismic traverse 3. Crops out in the central-southern Georgina Basin. Less than 650m thick. Glacial and periglacial deposit. Related to Sturt glaciation. Correlative to Sturt Tillite. Lateral equivalent to Mount Cornish Formation.||||Overlain disconformably by Black Stump Arkose. Underlain disconformably (inferred) with Yackah beds.|Green-grey diamictite and laminated siltstone with minor fine to very coarse (pebbly) grained quartz sandstone and arkose, locally capped by grey, laminated dolomitic shale and lenticular dolomite.|03-JUL-19
26242|Yardida Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
26242|Yardida Tillite|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump, Gnallan-a-gea and Sun Hill Arkoses and Little Burke Tillite, are all mapped under the symbol, -P-Cg.||||||
26242|Yardida Tillite|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 2.||Aroota Group.|||Glacial sedimentary rocks.|12-JUL-16
26242|Yardida Tillite|69439|6|Mentioned|p24:7|||Georgina Basin.||||Correlated with Naburula Formation (Ngalia Basin).||12-JUL-16
26242|Yardida Tillite|69443|4|Described|p28:5, 7-8, 33, 45|Cryogenian|Cryogenian|Walter (1980). Desert Syncline and Field River Anticline, SE Georgina Basin. Unfossiliferous. Generally recessive and poorly exposed. Thickness probably c.650m. Glacial and periglacial deposits with a (postglacial) cap carbonate. Exposed by Toomba Fault. A shale within this Formation contains TOC up to 0.90%.||Aroota Group.||Disconformably overlies Yackah beds. Is overlain disconformably by Black Stump Arkose. Correlated with Mount Cornish Formation.|Diamictite and laminated siltstone, and minor fine to vey coarse (to pebbly) quartz sandstone and arkose; locally capped by laminated dolomitic shale and lenticular dolostone up to 100m thick.|12-JUL-16
26242|Yardida Tillite|69591|5|Briefly described|p94|||Toko Syncline. Thickness is 100m in GSQ Mount Whelan 1, but up to 2900m in the NT. Correlated with Sturtian (lower) tillite in the Flinders Ranges (SA).||||Is overlain disconformably by Black Stump Arkose.|A glacigene deposit of highly variable thickness.|
26242|Yardida Tillite|69673|4|Described|p114 fig 92|Cryogenian|Cryogenian|Approximately 650m thick.||Aroota Group|||Diamictite, laminated siltstone and minor sandstone locally capped by dolomitic shale and dolostone.|
26242|Yardida Tillite|72516|6|Mentioned|p86|Cryogenian|Cryogenian|Georgina Basin.||||Equivalent to the Mount Cornish Formation.||02-JUN-21
26242|Yardida Tillite|73086|6|Mentioned|p62, p158|||Georgina Basin.||||Correlates to Areyonga Formation.||
24594|Yarman Formation|9531|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Langlovale Group.  Mudstone, siltstone and shale, scattered beds of sandstone.||||||
24594|Yarman Formation|23291|4|Described|p84 Tb. 3.6|Mesoproterozoic|Mesoproterozoic|Parent: Langlovale Group. Age: ~1550Ma. Thickness: At least 1800m. Geological Province: Georgetown Region.||||||08-JUL-15
24594|Yarman Formation|35921|2|Defined|p42|Mesoproterozoic|Mesoproterozoic|||||||
24594|Yarman Formation|36153|6|Mentioned|Fig.10|||||||||
24594|Yarman Formation|36216|6|Mentioned|p208|||||||||
24594|Yarman Formation|36780|6|Mentioned|Fig.10|||||||||
24594|Yarman Formation|36937|6|Mentioned|p229|||||||||
24594|Yarman Formation|37462|6|Mentioned|p273|||||||||
24594|Yarman Formation|37565|6|Mentioned|Fig.5|||||||||
24594|Yarman Formation|37570|4|Described|p116|||See also Fig.2||||||
24594|Yarman Formation|38716|4|Described|p193|||||||||
24594|Yarman Formation|39445|5|Briefly described|Table 2|||See also P37 & P45||||||
24594|Yarman Formation|39687|6|Mentioned|p1|||||||||
24594|Yarman Formation|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24594|Yarman Formation|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24594|Yarman Formation|41975|5|Briefly described|p438|||||||||
24594|Yarman Formation|43664|4|Described|p54|||||||||
24594|Yarman Formation|50627|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Langlovale Group.  Mudstone, siltstone and shale.||||||
24594|Yarman Formation|63866|5|Briefly described|p77|||Interpreted as a turbiditic facies associated with a prodeltaic system.||Langlovale Group||||
24594|Yarman Formation|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Georgetown Inlier.||||||
24594|Yarman Formation|67341|6|Mentioned|vi|||Croydon Subprovince, Etheridge Province.||||Is overlain by Malacura Sandstone.||
24594|Yarman Formation|68348|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.||Conformably overlies Malacura Sandstone.|Grey to maroon mudstone and siltstone; minor subfeldspathic to sublithic sandstone.|
24594|Yarman Formation|68349|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Savannah Province.||Unit in Langlovale Group.||Conformably overlies Malacura Sandstone.|Grey to maroon mudstone and siltstone; minor subfeldspathic to sublithic sandstone.|
24594|Yarman Formation|69591|4|Described|p61, p68, p70|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier. The type section is near a tributary of the Langdon River, SW of Red Bull Bore.||Langlovale Group.||Gradationally overlies Malacura Sandstone.|Massive to laminated mudstone with sporadic intervals in which sandstone beds that have characteristics of classic, prograded, distal turbidites are common.|
23294|Yarraden Schist|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Coen Metamorphic Group||||||12-JAN-05
23294|Yarraden Schist|22781|4|Described|p24|Proterozoic|Proterozoic|Coen Metamorphic Group||||||
23294|Yarraden Schist|23420|5|Briefly described|p 142 table 4.4|||In the Coen Metamorphic Group||||||
23294|Yarraden Schist|43738|6|Mentioned|p37|||||||||
23294|Yarraden Schist|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier. Dominant schist unit of the Group. Has smaller interbedded bodies of quartzite similar to the Mount Ryan Quartzite.||Coen Metamorphic Group.|||Sillimanite-mica-feldspar-quartz schist; some quartzite.|
23294|Yarraden Schist|71792|3|Fully described|p3, p5-p6, p8-p10, p13, p30|Mesoproterozoic|Paleoproterozoic|Coen Inlier, Savannah Province. Named for the Yarraden homestead and forms a north-northwest trending belt truncated by Permian Granites of the Weymouth Supersuite. Forms the bulk of the Coen Metamorphic Group in the Coen Inlier. Outcrops in the Ebagoola Shear Zone, west of Coen. The extent of this unit has been greatly expanded on the basis of lithological similarity and interpreted geophysical continuation. Metamorphic crystallisation ages of 426 and 417 Ma are provided. Contains a significant amount of rocks previously assigned as Holroyd and Sefton Metamorphics. Thickness is unknown and contacts with adjacent units are either gradational or faulted, with up to 2km of section preserved in some fault slices. In radiometrics is characterised by mottled, pinkish tones on ternary radiometrics. In magnetics it has a moderate response with some magnetic linears parallel to the main foliation. Intruded by Unit Dgk/9.|1646, 1653 and 1641 (Max. deposition ages)|Coen Metamorphic Group||Overlies the Mount Ryan Quartzite. Conformably (gradationally) overlain by the Lochs Gneiss. Intruded by the Wigan Adamellite.|Sillimanite-biotite-muscovite-quartz schist, hematite, chlorite with garnet in places. Contains some quartzite and rare conglomerate with quartzite boulders.|
23294|Yarraden Schist|71849|5|Briefly described|p8, p43, p46, p49, p74, p94, p108, p119|Mesoproterozoic|Paleoproterozoic|See also p195.||Coen Metamorphic Group.||Separates, and is intruded by, Morris, Emu Yard (inferred) and Meldrum Granites; and Rokeby Quartz Monzodiorite (inferred). Intruded by Tadpole Granite.||
23294|Yarraden Schist|71853|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.||In places gradational into Lochs Gneiss.|Sillimanite-biotite-muscovite-quartz schist; with hematite, chlorite, garnet in places.|
23294|Yarraden Schist|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.|||Sillimanite-biotite-muscovite-quartz schist; with hematite, chlorite, garnet in places.|
23294|Yarraden Schist|72983|4|Described|p5-7, p56, p91-102, p110, p116|Statherian|Statherian|Iron Range Province. Eastern Cape York region. Basal unit of the Coen Metamorphic Group. New ages led to two sampled outcrops mapped as Sefton Metamorphics being reassigned to this unit. Listed dates are maximum depositional ages. Metamorphic crystallisation ages of 426 +/- 9 Ma and 417 +/- 7 Ma. Records an early Mesoproterozoic [metamorphic] event between ~1560 Ma and 1530 Ma, and a late Silurian to Early Devonian event between ~425 Ma and ~415 Ma. Lacks prominent Grenvillian (1300-900 Ma) and Neoproterozoic detrital zircons.|1646 +/- 11 Ma, 1653 +/- 27 Ma SHRIMP U-Pb|Coen Metamorphic Group||Intruded by[?] Kintore Granite and Wigan Granite.|Northeast trending (quartz biotite sillimanite) schist and quartzite; veins of pegmatite and gneiss.|
27942|Yarraman Complex|23799|6|Mentioned|p78|||Includes the Boyne River granite (McTaggart, 1963).  Hill and Denmead included the Boondooma Igneous Complex as part of this unit (1960).  Geological Province: Yarraman Subprovince (Wandilla Province).||||||
27942|Yarraman Complex|45110|4|Described|p66|||See also P90.||||||
39834|Yarraman Sandstone Member|24613|2|Defined|p40-41|Frasnian|Frasnian|Of Stud Fm. Thickness: 200m in type section. In Burdekin Basin. Gradationally above and below into upper and lower redbed intervals of the Stud Fm. Dominant rock is fine- to med-gr. sublabile lithofeldspathic sandstone, calcareous in places details incl||||||18-JUL-14
39834|Yarraman Sandstone Member|43933|5|Briefly described|Map Legend||Late Devonian|Of Stud Formation.||||||
39834|Yarraman Sandstone Member|62522|2|Defined|p25-26|Frasnian|Frasnian|Of Stud Fm (Dotswood Gp). Formerly Yarraman Flagstone Wedge. Conformable on fine redbed interval of Stud Fm. Thickness: 200m. Sublabile lithofeldspathic ss dominates, calcareous in places; siltstone/mudst. more dominant in upper part. In Burdekin Basin.||||||
39834|Yarraman Sandstone Member|68731|5|Briefly described|p186|Late Devonian|Late Devonian|Paleocurrent data suggests a southern source. Age constrained by the parent Stud Formation.||Of the Stud Formation.|||Comprises an interval dominated by coarse sandstone.|18-JUL-14
35196|Yarravale Creek Granite|23042|5|Briefly described|p100-105, Fig 2|Early Permian|Carboniferous|Intrudes Teemburra Igneous Complex.||||||
35196|Yarravale Creek Granite|60787|5|Briefly described|p9|Carboniferous|Carboniferous|||||||
35196|Yarravale Creek Granite|61917|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Pale pink to pale brown, medium- to coarse-grained hornblende granite and granodiorite; light grey, chlorite-altered, coarse-grained, porphyritic biotite-hornblende tonalite; common porphyritic andesite, rhyolite, microgranite and aplite dykes.||||||16-MAR-06
35196|Yarravale Creek Granite|65388|2|Defined|p389-390, 135, 362, 364, 365,380 386,388|Early Permian|Late Carboniferous|Northern Connors Arch. Southern Urannah Batholith. Probably intrudes Teemburra Igneous Complex, Pisgah Igneous Complex. Probable age given. Pale to deep pink, medium-grained, porphyritic biotite granite in type section; porphyritic syenogranite in nthn body.||||||
76897|Yarrie Rock Waterhole Granite|67323|5|Briefly described|GIS attrib tbl, p7|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Age said to be unknown p7.||Sybella Suite||Intrudes Oroopo Metabasalt.|Deeply weathered muscovite-biotite granite; schlieren-rich; grades into pink to cream, garnet-bearing, aplitic granite|
76897|Yarrie Rock Waterhole Granite|69591|5|Briefly described|p59|||Sybella Batholith.|||||Deeply weathered muscovite-biotite granite; schlieren-rich; grades into pink to cream, garnet-bearing aplitic granite.|
27943|Yarrol Formation|22973|5|Briefly described|p9 Fig.2 (b)|Early Permian|Early Permian|||||||
27943|Yarrol Formation|23468|5|Briefly described|Fig 2 p 295|||||||||
27943|Yarrol Formation|24076|5|Briefly described|p397 Fig. 2|Early Permian|Early Permian|Max. thickness: 520m.  Geological Province: Yarrol Basin.||||||
27943|Yarrol Formation|24488|5|Briefly described|Map Legend|Permian|Permian|||||||
27943|Yarrol Formation|24491|5|Briefly described|p14|Early Permian|Namurian|||||||
27943|Yarrol Formation|24615|5|Briefly described|CD|Permian|Permian|[Pa].  sandstone. siltstone, limestone, chert, minor andesite.||||||
27943|Yarrol Formation|29437|6|Mentioned|p136|||||||||
27943|Yarrol Formation|30449|6|Mentioned|p6|||Lower Permian. Brachiopods||||||
27943|Yarrol Formation|30450|6|Mentioned|Table 1|||Permian age. Yarrol Basin.||||||
27943|Yarrol Formation|30451|4|Described|p40|||See also P41||||||
27943|Yarrol Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
27943|Yarrol Formation|31659|6|Mentioned|Table 2|||Correlation||||||
27943|Yarrol Formation|32943|6|Mentioned|p106|||||||||
27943|Yarrol Formation|32945|6|Mentioned|Fig.1|||Permian||||||
27943|Yarrol Formation|34132|6|Mentioned|p4|||Lower Permian||||||
27943|Yarrol Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
27943|Yarrol Formation|34348|6|Mentioned|p19|||||||||
27943|Yarrol Formation|36045|6|Mentioned|p332|||||||||
27943|Yarrol Formation|36925|6|Mentioned|p180|||||||||
27943|Yarrol Formation|37109|5|Briefly described|p283|||||||||
27943|Yarrol Formation|38204|6|Mentioned|p77|||||||||
27943|Yarrol Formation|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
27943|Yarrol Formation|39252|6|Mentioned|p21|||||||||
27943|Yarrol Formation|39445|5|Briefly described|Table 8|||||||||
27943|Yarrol Formation|40623|5|Briefly described|p79|||||||||
27943|Yarrol Formation|40997|6|Mentioned|p415|||||||||
27943|Yarrol Formation|41246|6|Mentioned|Map legend|Permian||||||||
27943|Yarrol Formation|42547|5|Briefly described|p53|||||||||
27943|Yarrol Formation|43017|5|Briefly described|Fig.3,p375|||||||||
27943|Yarrol Formation|43471|14|Not recorded|p242|||Megadesmus, Astartila discussed||||||
27943|Yarrol Formation|43474|14|Not recorded|p7||Artinskian|||||||
27943|Yarrol Formation|43475|14|Not recorded|p553||Permian|||||||
27943|Yarrol Formation|43882|14|Not recorded|p87,88,90||Early Permian|||||||
27943|Yarrol Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
27943|Yarrol Formation|43983|14|Not recorded|p8|||||||||
27943|Yarrol Formation|43998|4|Described|p19||Early Permian|||||||
27943|Yarrol Formation|44091|14|Not recorded|p44,47,Tb.3||Permian|||||||
27943|Yarrol Formation|44360|14|Not recorded|p16,18||Early Permian|||||||
27943|Yarrol Formation|44369|2|Defined|Tb.6,p169,171|||Limestone, subgreywacke.||||||
27943|Yarrol Formation|44370|2|Defined|p217-220|||||||||
27943|Yarrol Formation|44372|6|Mentioned|p5-7||Early Permian|Overlies Burnett Formation. Underlies Owl Gully Formation.||||||
27943|Yarrol Formation|44378|14|Not recorded|p199||Artinskian|6 miles E S E of Cania, in Yarrol Basin. (Probably Early Artinskian)||||||
27943|Yarrol Formation|44379|4|Described|p1,2,16,18-20,Tb.3,||Early Permian|Map. Ref. to Maxwell 1959.||||||
27943|Yarrol Formation|44515|2|Defined|p30,31||Sakmarian|Fossils.||||||
27943|Yarrol Formation|45031|14|Not recorded|p51,52,72||Permian|||||||
27943|Yarrol Formation|63832|6|Mentioned|p131 fig 2|Artinskian|Artinskian|Of east Bowen Basin. Sixth (P2) glaciation.||||||
27943|Yarrol Formation|64631|5|Briefly described|p44 Fig.2.|Artinskian|Artinskian|?Northern New England Fold Belt. Biostratigraphic age control for base and top.||||Overlies Youlambie Conglomerate. Is overlain by Owl Gully Volcanics.||
27943|Yarrol Formation|65388|6|Mentioned|p164, 178, 186|Early Permian||Yarrol Province. Reflects early Permian marine transgression, as does Buffel Formation and Tiverton Formation.||||||
27943|Yarrol Formation|68008|3|Fully described|p121, p123, p132-134, p136, p138, p140|Permian|Permian|See also p147, p163, p569. Defined in the Yarrol Syncline by Maxwell (1959); extended to the Spring Creek Syncline by Dear (1968), and N of Biloela by Dear et al. (1971). The type area is in the vicinity of Yarrol homestead on the Burnett River (Maxwell, 1960) where it is 515m thick. Forms strike ridges. Fossil species listed: Artinskian age. Age-correlative of lower Rookwood Volcanics, but lithologies differ.||||Conformably overlies Lorray Formation, Youlambie Conglomerate. Is overlain conformably by Owl Gully Volcanics or Smoky beds. Time-correlative of Lakes Creek Formation.|Grey, detrital, fossiliferous limestone grading into richly fossiliferous coquinitic silty limestone and calcareous siltstone; dark siltstone and sandstone, usually calcareous; greyish-green chert; local interbedded andesitic lavas near top.|
27943|Yarrol Formation|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Yarrol Province. ||||||
27943|Yarrol Formation|68679|5|Briefly described|p312-313, p338, p341-342, p380|Artinskian|Artinskian|Maxwell (1959). Northern New England Orogen.|||||Detrital limestone with abundant fossils grading into richly fossiliferous coquinitic silty limestone and calcareous siltstone, siltstone, lithic sandstone, chert; local andesite lavas towards the top.|
38886|Yarwun beds|24420|5|Briefly described|p6|Early Carboniferous|Late Devonian|||||||
38886|Yarwun beds|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
38886|Yarwun beds|24615|5|Briefly described|CD|Carboniferous|Devonian|[DCy].  Interbedded sandstone and siltstone, dacitic to rhyolitic volcaniclastic conglomerate with rip-up clasts.||||||
38886|Yarwun beds|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
38886|Yarwun beds|50208|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
38886|Yarwun beds|61778|6|Mentioned|p234 Fig. 1, p241|Early Carboniferous|Late Devonian|Geological Province: Berserker Subprovince.||||||07-FEB-11
38886|Yarwun beds|64429|5|Briefly described|p16 Fig.1|Carboniferous|Devonian|Chalmers Formation is faulted against these rocks.||||||
26245|Yataga Granodiorite|9539|5|Briefly described|Map legend|Permian|Permian|Grey to pink biotite and hornblende-biotite granodiorite, locally porphyritic; dark grey hornblende-biotite granodiorite and tonalite.||||||
26245|Yataga Granodiorite|23291|3|Fully described|p45-46, p96 Table 3.11|Early Permian|Early Permian|Intrudes the Etheridge Group with a metamorphic aureole up to 500m wide. Parent: Yataga Supersuite. Geological Province: Georgetown Region.||||||29-MAY-15
26245|Yataga Granodiorite|23510|5|Briefly described|Map Legend||Early Permian|of Yataga Supersuite.||||||
26245|Yataga Granodiorite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 8. I-Type.||||||
26245|Yataga Granodiorite|33909|2|Defined|p231|Permian|Carboniferous|Permian or Carboniferous||||||
26245|Yataga Granodiorite|35214|6|Mentioned|p8|||||||||
26245|Yataga Granodiorite|35920|6|Mentioned|p25|||||||||
26245|Yataga Granodiorite|39445|5|Briefly described|Table 12|||See also P90||||||
26245|Yataga Granodiorite|39917|6|Mentioned|Map legend|Permian|Permian|||||||
26245|Yataga Granodiorite|40860|6|Mentioned|p113|||||||||
26245|Yataga Granodiorite|43259|4|Described|Appendix 1,p16.||Permian|||||||
26245|Yataga Granodiorite|43664|6|Mentioned|p96|||||||||
26245|Yataga Granodiorite|43740|3|Fully described|p32||Carboniferous|||||||
26245|Yataga Granodiorite|50198|5|Briefly described|Map Legend|Early Permian|Early Permian|||||||
26245|Yataga Granodiorite|68354|5|Briefly described|Map legend.|Early Permian|Early Permian|Kennedy Province. The outer zone of this circular stock indicates reversed polarity remnant magnetisation.|||||Dark grey hornblende-biotite granodiorite and tonalite; grey to pink biotite and hornblende-biotite granite and granodiorite, locally porphyritic; minor pink aplite.|
26245|Yataga Granodiorite|69593|5|Briefly described|p484, p511|||Kidston Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|320-280 Ma.|Yates Supersuite.|||Hornblende-biotite granodiorite to biotite granite and leucogranite. I-type.|
36272|Yataga Supersuite|23291|5|Briefly described|p45, p96 Tb. 3.11|Early Permian|Early Permian|Geological Province: Georgetown Region.||||||08-JUL-15
36272|Yataga Supersuite|23510|5|Briefly described|Map Legend||Early Permian|||||||
36272|Yataga Supersuite|69593|5|Briefly described|p485, p489, p511|||Kidston, Herberton and/or Tate Subprovinces, Kennedy Igneous Association.|||Yataga Granodiorite.|||
69495|Yates Creek Basalt|68336|5|Briefly described|Map legend.|Quaternary|Quaternary|Nulla Basalt Province.|||||Olivine basalt.|
69495|Yates Creek Basalt|68339|5|Briefly described|Map legend.|Quaternary|Quaternary||0.7 - 0.64 Ma.||||Olivine basalt.|
69495|Yates Creek Basalt|68340|5|Briefly described|Map legend.|Quaternary|Quaternary||0.7 - 0.64 Ma.||||Olivine basalt.|
69495|Yates Creek Basalt|68341|5|Briefly described|Map legend.|Quaternary|Quaternary|Nulla Basalt Province.|||||Olivine basalt.|
69495|Yates Creek Basalt|68478|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Middle Pleistocene age.|0.64-0.7 Ma||||Olivine basalt.|
69495|Yates Creek Basalt|68479|5|Briefly described|Map Legend|Pleistocene|Pleistocene||0.64-0.7 Ma||||Olivine basalt.|
69495|Yates Creek Basalt|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Barkers Basalt; the Maer Volcanics; parts of the McBride and Nulla Basalt Groups, and unnamed basalt flows, are all mapped under the symbol, Qbn.||||||
69495|Yates Creek Basalt|73115|6|Mentioned|p: 76-77, 90, 94, 99, 105, 110, 115, 120|Pleistocene|Pleistocene|Nulla Basalt Province.|0.64-0.7 Ma|||||
69329|Yates Suite|60425|5|Briefly described|p272-3 Appdx. 1|Late Permian|Late Permian|Of Yates Supersuite. Contains Mount Yates Granodiorite. I-type.||||||07-FEB-11
41336|Yeldham Suite|50536|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Age: 1820Ma.||||||07-NOV-08
24599|Yellow Waterhole Granite|22483|5|Briefly described|p425.|||||||||
24599|Yellow Waterhole Granite|22515|3|Fully described|Fig1p398,402-3|Calymmian|Calymmian|U-Pb zircon age of 1492 (+/-) 11 Ma (Page 1993); K-Ar biotite mineral age of 1458 Ma (Richards et al. 1963).||||||
24599|Yellow Waterhole Granite|22667|6|Mentioned|Fig1 p234, p238||Calymmian|Age of unit is 1465+/-16 Ma.||||||15-MAR-07
24599|Yellow Waterhole Granite|23064|6|Mentioned|136|||||||||
24599|Yellow Waterhole Granite|23471|5|Briefly described|p110 Fig 1|Calymmian|Calymmian|Age: 1510+/-8 Ma (U-Pb SHRIMP). Geological Province: Mount Isa Block.||||||
24599|Yellow Waterhole Granite|23967|6|Mentioned|p1331|||||||||
24599|Yellow Waterhole Granite|23974|5|Briefly described|p1452 Fig. 2a|Proterozoic|Proterozoic|Geological Province: Selwyn Region.  Age: 1493 +/- 8Ma.||||||
24599|Yellow Waterhole Granite|24197|5|Briefly described|p95 Tb. 12.1|Mesoproterozoic|Mesoproterozoic|Of the Williams Supersuite. Age: 1510Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
24599|Yellow Waterhole Granite|24256|5|Briefly described|p48 Fig.1|Calymmian|Calymmian|Geological Province: Mount Isa Block. Age: ~1504-1482Ma (U-Pb)||||||
24599|Yellow Waterhole Granite|24257|6|Mentioned|p65 Fig. 1|||Geological Province: Eastern fold belt, Mount Isa Block.||||||
24599|Yellow Waterhole Granite|24258|6|Mentioned|p89 Fig. 3|||Geological Province: Mount Isa Inlier||||||
24599|Yellow Waterhole Granite|37862|4|Described|p589|||||||||
24599|Yellow Waterhole Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24599|Yellow Waterhole Granite|38658|6|Mentioned|p153|||||||||
24599|Yellow Waterhole Granite|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
24599|Yellow Waterhole Granite|39445|6|Mentioned|Table 2|||||||||
24599|Yellow Waterhole Granite|40840|6|Mentioned|Map legend|||||||||
24599|Yellow Waterhole Granite|41306|6|Mentioned|p4|||See also p9.||||||15-MAR-07
24599|Yellow Waterhole Granite|41979|5|Briefly described|p532|||||||||
24599|Yellow Waterhole Granite|43490|6|Mentioned|8|||U-Pb Zircon Age: 1493+/-8Ma||||||
24599|Yellow Waterhole Granite|44195|5|Briefly described|p345 Table 1,355|||U-Pb age: 1493+/-8 Ma. See also p358.||||||15-MAR-07
24599|Yellow Waterhole Granite|45161|5|Briefly described|p52|||||||||
24599|Yellow Waterhole Granite|45166|5|Briefly described|p39|||||||||
24599|Yellow Waterhole Granite|49009|2|Defined|p53|Proterozoic|Proterozoic|Mapped as Williams Granite by Carter & Opik (1963).||||||
24599|Yellow Waterhole Granite|50100|5|Briefly described|p21, p61|Calymmian|Calymmian|Of the Williams Supersuite.||||||
24599|Yellow Waterhole Granite|50536|5|Briefly described|p1.5, 10.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier. Of the Williams Suite/Supersuite. Age: 1493 +/- 8Ma (SHRIMP).||||||19-MAR-18
24599|Yellow Waterhole Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite and hornblende-biotite granite.||||||
24599|Yellow Waterhole Granite|60658|6|Mentioned|p61|||Granite pluton. Geological Province: Eastern Fold Belt / Mount Isa Inlier||||||15-MAR-07
24599|Yellow Waterhole Granite|61927|5|Briefly described|p96|Mesoproterozoic|Mesoproterozoic|Intrusion of undeformed  granite. Age: 1493+/-8 Ma.||||||17-APR-12
24599|Yellow Waterhole Granite|61933|5|Briefly described|p169 Fig.1|Mesoproterozoic|Mesoproterozoic|Pluton of the Williams and Naraku Batholiths -age: 1516-1490 Ma.||||||15-MAR-07
24599|Yellow Waterhole Granite|61936|5|Briefly described|p200|||A-type, metaluminous, magnetite-bearing plutonic rocks of the Isan Orogeny. ||||||
24599|Yellow Waterhole Granite|63866|5|Briefly described|p64||||1493 +/- 8 Ma (Page and Sun, 1998)|||||
24599|Yellow Waterhole Granite|64248|6|Mentioned|p33 Fig.1, p45|||Appears as Yellow Water Hole Granite on p45.||||||11-DEC-17
24599|Yellow Waterhole Granite|64250|6|Mentioned|p10 fig 2, p11 fig 3, p15|Calymmian|Calymmian||1493 +/-8 Ma|||||13-MAY-14
24599|Yellow Waterhole Granite|65396|5|Briefly described|p7, p22, p40, p53, p56, p61, p82, p99|Calymmian|Calymmian|See also p121, p147, p157, p160, p173, p175, p182, p213, p224, p241, p272, p360-361, p438, p440, p445, p474-500. Kalkadoon-Leichhardt Belt. Eastern succession. Appears as Yellow Water Hole Granite on p22 and p224. Geochronology by Pollard and McNaughton (1997), and Page and Sun (1998), respectively. Stress partitioning and fluid flow models detailed.|1510 +/- 8 Ma, 1493 +/- 8 Ma|||||
24599|Yellow Waterhole Granite|66913|5|Briefly described|p170 fig 1, p171 fig 2, p173, p188|Calymmian|Calymmian|U-Pb zircon SHRIMP ages shown diagramatically on Fig. 2.|1493 +/- 8 Ma from strongly albitised sample.|||||
24599|Yellow Waterhole Granite|67323|4|Described|GIS attrib tbl, Solid Geology Map, p19|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot. Kuridala-Selwyn Domain, Mount Isa Inlier. Williams Igneous Event. Higher magnetic response.|1510 +/- 8 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.||Intrudes Kuridala Group.|Non-porphyritic and porphyritic hornblende-biotite and biotite granite; minor aplite.|
24599|Yellow Waterhole Granite|68542|6|Mentioned|p18|||||||||
24599|Yellow Waterhole Granite|68576|6|Mentioned|Q_2: p16, p18|||An intrusive phase of the 1545-1500 Ma Williams/Naraku Batholith, S of Cloncurry.||||||
24599|Yellow Waterhole Granite|69377|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Equigranular to porphyritic hornblende-biotite granite, minor equigranular granite, pyroxene-bearing granite and aplite|
24599|Yellow Waterhole Granite|69378|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|||Williams Supersuite|||Equigranular to porphyritic hornblende-biotite and biotite granite, minor aplite|
24599|Yellow Waterhole Granite|69549|6|Mentioned|p95|Calymmian|Calymmian|Shown as Yellow Waterhole granite.|1493 +/- 8 Ma.|||||
24599|Yellow Waterhole Granite|69591|5|Briefly described|p51, p59|||Eastern Mount Isa Province; late Isan Orogeny.|1510 +/- 8 Ma (Pollard and McNaughton, 1997).|Williams Supersuite.|||A-type granitoid.|
24599|Yellow Waterhole Granite|70572|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular to porphyritic Hornblende-biotite and biotite granite; minor aplite.|20-JAN-22
24599|Yellow Waterhole Granite|70573|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Kuridala-Selwyn Domain.||Williams Supersuite|||Equigranular-porphyritic hornblende-biotite and biotite granite; minor aplite.
|
24599|Yellow Waterhole Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1493+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
24599|Yellow Waterhole Granite|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.|1493 +/- 8 Ma|||||
24599|Yellow Waterhole Granite|72949|6|Mentioned|p35|Calymmian|Calymmian|Mount Isa Inlier, Western Fold Belt.||||||
24599|Yellow Waterhole Granite|73413|6|Mentioned|p3|Calymmian|Calymmian|Mount Isa Inlier, Eastern Fold Belt.|1510 +/- 10 Ma, 1493 +/- 8 Ma|||||
24599|Yellow Waterhole Granite|73525|5|Briefly described|p4-5 Fig.2|Calymmian|Calymmian|Kuridala-Selwyn-Marimo-Doherty Domain.|1510+/-8 Ma crystallisation age||||Felsic intrusive.|
28039|Yellowood Granodiorite|23420|6|Mentioned|p 148 table 4.7|||Also see Yellow Granodiorite||||||
28039|Yellowood Granodiorite|43596|4|Described|p25,  p26 Tb. 2|||Of Flyspeck Supersuite. Intrudes Sugarbag Creek Quartzite, Astrea and Dinah Formations and Gumhole Monzogranite. Hornblende-biotite granodiorite and minor biotite granodiorite to monzogranite; +scattered enclaves of melanocratic microdiorite/tonalite.||||||27-JAN-09
28039|Yellowood Granodiorite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
28039|Yellowood Granodiorite|71849|6|Mentioned|p172|||REE distribution pattern shown to contrast with Rokeby Quartz Monzodiorite.||Flyspeck Supersuite.||||
24141|Yenda Granodiorite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
24141|Yenda Granodiorite|40919|6|Mentioned|Fig.2|||||||||
24141|Yenda Granodiorite|41778|2|Defined|Table 1|Triassic|Permian|Described P372||||||
24141|Yenda Granodiorite|41824|6|Mentioned|p201|||||||||
24141|Yenda Granodiorite|42054|6|Mentioned|p273|||||||||
24141|Yenda Granodiorite|43008|5|Briefly described|map legend|||||||||
24141|Yenda Granodiorite|63821|5|Briefly described|p29|Triassic|Permian|Intrudes Curtis Island Group. Forms a zoned intrusion with an outer zone of diorite and successive inner zones of granodiorite, adamellite and granite.||||||07-FEB-11
24141|Yenda Granodiorite|68679|5|Briefly described|p420-422|||Gayndah-Gladstone belt. May be continuous with the lithologically similar Briggs Granodiorite, but displaced 7km on the Perry Fault.||||Is adjacent to Mingo Granite.|Biotite-hornblende granite to granodiorite. I-type.|
41249|Yerilla Metamorphics|50598|5|Briefly described|Map Legend|Carboniferous|Devonian|Biotite gneiss, mica schist, amphibolite, migmatite, strongly deformed granitoids, metabasalt.||||||
41249|Yerilla Metamorphics|61087|5|Briefly described|Map Legend|Carboniferous|Devonian|Biotite gneiss, mica schist, amphibolite, migmatite and strongly deformed granitoids. Undivided metmorphic rocks.||||||
41249|Yerilla Metamorphics|65388|3|Fully described|p10-13; p11, 43, 46, 236, 239, 240, 251|Early Carboniferous||Age is unknown. Intruded by Evandale Tonalite, orthogneiss dated at 342.5+/- 4.0 Ma, dykes of Horse Leucogneiss, and late Carboniferous Glisson Granodiorite. Unconformably overlain by the early Permian Narayen beds. See also p258, 329, 432.||||||
41249|Yerilla Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Auburn Subprovince.||||||
41249|Yerilla Metamorphics|68679|5|Briefly described|p312-313, p344, p352-354, p405,p407,p419|Carboniferous|Late Devonian|Auburn Arch (Subprovince), northern New England Orogen. Crops out over ~120 km2, WNW of Mundubbera and in scattered areas S along the Auburn River. Age unknown, but intruded by 342.5 +/- 4 Ma orthogneiss (Fanning et al.,2009).||||Is faulted against the Narayen beds. Is intruded by Jack Shay, Quaggy Mountain Gabbros; Evandale Tonalite; Pollard and Glissons Granodiorites; Wathonga Granite (probably).|Metasedimentary and mafic metavolcanics are intruded by variably foliated granitoids: orthogneiss, common pegmatite and aplite, younger granite, diorite and gabbro, dolerite and rhyolite dykes. Biotite schist and paragneiss grade into migmatite.|
23306|Yering Granodiorite|23032|5|Briefly described|p41|||||||||
23306|Yering Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
23306|Yering Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
23306|Yering Granodiorite|43480|2|Defined|7-38|Devonian|Silurian|Age: 407Ma||||||
23306|Yering Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Pink, pinkish-grey or grey, fine to med.-gr.seriate muscovite-biotite granodiorite, with sparse feldspar phenocrysts to 4mm and common quartz phenocrysts to 4mm; common angular to rounded biotite-rich enclaves and diffuse schleiren.||||||
23306|Yering Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Pink to grey, fine- to medium-grained seriate muscovite-biotite granodiorite, with sparse feldspar phenocrysts to 4 mm and common quartz phenocrysts to 4 mm; common angular to rounded biotite-rich enclaves and diffuse schlieren.|
23306|Yering Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Pink, pinkish-grey or grey, fine to medium-grained seriate muscovite-biotite granodiorite, with sparse feldspar phenocrysts to 4 mm and common quartz phenocrysts to 4 mm; common angular to rounded biotite-rich enclaves and diffuse schlieren.|
23306|Yering Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian |Reedy Springs Batholith, Pama Province.|||||Pink, pinkish-grey or grey, fine to medium-grained seriate muscovite-biotite granodiorite, with sparse feldspar phenocrysts to 4 mm and common quartz phenocrysts to 4 mm; common angular to rounded biotite-rich enclaves and diffuse schlieren.|
23306|Yering Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
24143|Yokas Microgranite|23423|5|Briefly described|p315 Table 7.4||Early Permian|Of Lags Supersuite.||||||01-JUN-09
24143|Yokas Microgranite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No.  425. A-Type.||||||
24143|Yokas Microgranite|23713|5|Briefly described|p71 Appendix 2|||Intrudes Nightflower Dacite and Wakara Volcanic Subgroup. Of Lags Supersuite.||||||
24143|Yokas Microgranite|42681|4|Described|p21|||||||||
24143|Yokas Microgranite|43083|5|Briefly described|p259|||Of Lags Supersuite. A-type.  Lithology included.||||||17-JUN-09
24143|Yokas Microgranite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Pale grey to red-brown, strongly porphyritic garnet-hornblende microgranite.||||||15-JUN-06
24143|Yokas Microgranite|43254|5|Briefly described|map legend||Early Permian|Of Lags Supersuite.||||||01-JUN-09
24143|Yokas Microgranite|43259|4|Described|Appendix 1,p46.||Permian|||||||
24143|Yokas Microgranite|43625|6|Mentioned|p34|||||||||
24143|Yokas Microgranite|43626|6|Mentioned|p72|||||||||
24143|Yokas Microgranite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province. Pale grey to reddish brown, highly porphyritic garnet-hornblende microgranite; generally extenively altered.||||||
24143|Yokas Microgranite|60425|4|Described|p45 Tb. 3, p58 Tb. 4, p276-7 Appdx. |Early Permian|Early Permian|Of Lags Suite (Lags Supersuite). Intrudes Wakara Volcanic Subgroup (Featherbed Volcanic Group). A-type. Pale grey-red brown, very fine-grained, highly porphyritic garnet-hornblende microgranite, with embayed quartz phenocrysts; extensively altered.||||||07-FEB-11
24143|Yokas Microgranite|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Lags Suite.|||A-type.|
27971|Yongala Volcanic Subgroup|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
27971|Yongala Volcanic Subgroup|23423|4|Described|p305 Table 7.3||Early Permian|Age: 288+/-17 Ma, 290+/-12 Ma, 284+/-4 Ma  (Rb-Sr). Featherbed Volcanic Group. Underlying unit James Creek Granite, Rock Hole Rhyolite (unconformable).||||||
27971|Yongala Volcanic Subgroup|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group.||||||
27971|Yongala Volcanic Subgroup|23501|6|Mentioned|map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group & Lags Supersuite.||||||
27971|Yongala Volcanic Subgroup|23616|5|Briefly described|Table 3 p47||Permian|Age: 288+/-17 Ma, 290+/-12 Ma (Rb-Sr). Of Featherbed Volcanic Group. Max thickness ~2500-3000 m.||||||
27971|Yongala Volcanic Subgroup|23713|5|Briefly described|p33||Early Permian|Of Featherbed Volcanic Group||||||
27971|Yongala Volcanic Subgroup|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Featherbed Volcanic Group.||||||15-JUN-06
27971|Yongala Volcanic Subgroup|43254|5|Briefly described|map legend||Early Permian|of Featherbed Volcanic Group.||||||
27971|Yongala Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p11.||Early Permian|||||||
27971|Yongala Volcanic Subgroup|43626|4|Described|p43|Early Permian|Late Carboniferous|||||||
27971|Yongala Volcanic Subgroup|44246|5|Briefly described|Map Legend||Early Permian|||||||
27971|Yongala Volcanic Subgroup|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||
27971|Yongala Volcanic Subgroup|60425|3|Fully described|p45 Tb. 3, p46 Tb. 3|Early Permian|Early Permian|Of Featherbed Volcanic Group. Contains the Arringunna, Combella and Fisherman Rhyolites. Unconformably overlain by Wollenden Rhyolite (Wakara Volcanic Subgp). Cut by Saint Helena Monzogranite and Yokas Microgranite.||||||07-FEB-11
27971|Yongala Volcanic Subgroup|62523|4|Described|p9, p3-4 (map/legend)|Early Permian|Late Carboniferous|Of Featherbed Volcanic Group. Comprises the unit at the base of the Djungan Cauldron, a major component within the Featherbed Cauldron Complex. Previously of the "Featherbed Volcanics". Includes the Fisherman Rhyolite and Maneater Granodiorite.||||||07-FEB-11
27971|Yongala Volcanic Subgroup|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Featherbed Volcanic Group.|Includes Fisherman, Combella and Arringulla Rhyolites.|||
27971|Yongala Volcanic Subgroup|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.|||A-type.|
36430|Yuccabine Granodiorite|23617|4|Described|Table 2 p16||Early Permian|282 Ma (SHRIMP). Also see p31-32. Name refers to granodiorite exposed north-west of Mount Collins in the Kirrama Range. Kennedy Province.||||||
36430|Yuccabine Granodiorite|23618|5|Briefly described|map legend||Early Permian|||||||
36430|Yuccabine Granodiorite|69593|5|Briefly described|p495, p512|Permian|Early Carboniferous|Ingham Batholith. Sm-Nd isotope data tabulated.|282 +/- 4 Ma.||||I-type.|
24145|Yulga Tonalite|22847|3|Fully described|p 52|Early Devonian|Late Silurian|||||||
24145|Yulga Tonalite|23422|5|Briefly described|p213 Table 6.8|||||||||
24145|Yulga Tonalite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 118. I-Type.||||||
24145|Yulga Tonalite|42245|2|Defined|p37|Early Devonian|Late Silurian|||||||
24145|Yulga Tonalite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
24145|Yulga Tonalite|43259|4|Described|Appendix 1,p23.|Early Devonian|Late Silurian|Late Silurian - Early Devonian?.||||||
24145|Yulga Tonalite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
24145|Yulga Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Yulga ton.||Unit in Millchester Supersuite.||||
39597|Zig Zag Tonalite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
39597|Zig Zag Tonalite|50197|5|Briefly described|Map Legend|Triassic|Permian|||||||
39597|Zig Zag Tonalite|68008|3|Fully described|p334-335, p421-424|Triassic|Permian|Delineated but not described by exploration company mapping. A small (2 x 1 km) oval pluton 40km W of Calliope. The type area is a low ridge W of Zig Zag Creek (after which the unit is named), where the tonalite forms sparse boulders. Mostly devoid of outcrop. Geophysics briefly described. Geochemistry mentioned. No age determination.||||Intrudes Mount Alma Formation and Rockhampton Group.|Pale grey, medium-grained, equigranular hornblende-biotite tonalite.|
39597|Zig Zag Tonalite|68679|5|Briefly described|p425, p427|||Yarrol Province. A ~2 x 1 km oval intrusion just N of Galloway Plains Igneous Complex. Geochemistry briefly described.||||Intrudes Mount Alma Formation and Rockhampton Group.|Hornblende-biotite tonalite.|
83361|Zig Zag dyke|72983|5|Briefly described|p5, p7, p70-75|Kungurian|Artinskian|[informal unit name; also referred to as the Zig Zag rhyolite dyke, p75]. Etheridge Province, Kennedy Igneous Association. Georgetown region. Hosted within the Zig Zag Fault. Linked with mineralised sills within the Sherwood gold deposit.|284.5 +/- 1.4 Ma SHRIMP U-Pb|Agate Creek Volcanic Group (inferred)|||Aphanitic rhyolite.|31-AUG-22
33727|black soil 33727|44483|5|Briefly described|map legend|Cenozoic|Cenozoic|Black soil.||||||19-NOV-08
78469|granite - low magnetic intensity 78469|69042|6|Mentioned|map legends|Devonian|Silurian|NMG. Areas of granites (both S-type and some I-types) having low magnetic intensity.||||||
