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
81885|ABC range Quartzite|72451|4|Described|p4|Late Proterozoic|Late Proterozoic|Contains much crossbedding, ripple marks, mud cracks and shale chip conglomerates indicating a marginal marine environment grading from sub-tidal to inter-tidal up sequence.  Diachronous with the Brachina Formation. See also ABC Range Quartzite, all p4. Defines the weathering resistant ridgeline and small cliffs of the prominent first ridge of the ABC Range.||||Overlain by Bunyeroo Formation.|Pale pinkish grey fine to medium grained quartzite with minor micaceous siltstone partings|09-JUN-20
35882|Abminga Subsuite volcanics|23347|6|Mentioned|p52|||Informal - see Abminga Subsuite. Characterises Curnamona Group by its presence.||||||24-MAR-09
35882|Abminga Subsuite volcanics|60485|6|Mentioned|p26|Statherian|Statherian|Informal name.  Of the Basso Suite.  Age: ~1715-1710Ma.||||||03-MAR-05
75089|Abminga metavolcanic""|22884|5|Briefly described|p40 Fig. 1|||A discrete plagioclase-rich unit at or near the base of George Mine Formation; contains relict quartz phenocrysts; forms a distinct marker unit.||||||
69592|Abrakarrie Limestone|61155|5|Briefly described|p17|Early Miocene|Late Oligocene|Misspelt - see Abrakurrie Limestone (place-name is Abrakurrie Cave in WA). Age: 25-20.5Ma. Max. thickness: 90m. Geological Province: Eucla Basin.||||||
82253|Abraukurrie Limestone|73112|5|Briefly described|Map legend.|||[Mis-spelling of Abrakurrie].||||Is overlain locally by Nullarbor Limestone.|Yellowish bryozoan limestone.|
39582|Aclare Pyrite Beds|24465|5|Briefly described|p346 Fig.3|||Of Mirams, 1962 - as part of the Brown Hills Subgroup.   Probably superseded.||||||19-JAN-05
81286|Acraman impact ejecta layer''|68271|6|Mentioned|p697|||||||||
41667|Acropolis dacite|50605|5|Briefly described|p8.1|Mesoproterozoic|Mesoproterozoic|Of the Hiltaba Supersuite. Age: 1591-1578 +/- 13Ma (U-Pb). Geological Province: Gawler Craton & Curnamona Province.||||||
80383|Adelaide "Series"|71242|14|Not recorded|p9|||||||||
31369|Adelaide Rift Complex|23314|6|Mentioned|329|||||||||
31369|Adelaide Rift Complex|24570|6|Mentioned|p399|||||||||
31369|Adelaide Rift Complex|43560|5|Briefly described|p223|||Probably structural term not stratigraphic name.||||||
31369|Adelaide Rift Complex|50127|6|Mentioned|p48 Fig. 2|||Structural term.||||||
31369|Adelaide Rift Complex|50327|5|Briefly described|p300, p303, p305|Neoproterozoic|Neoproterozoic|More structural terminology than stratigraphical. In South Australia. Includes Skillogalee Dolomite, Nuccaleena Formation and Tindelpina Shale Member.||||||07-FEB-11
31369|Adelaide Rift Complex|60900|6|Mentioned|p897|Adelaidean|Adelaidean|||||||
31369|Adelaide Rift Complex|63020|5|Briefly described|p971|||In Mt Lofty Ranges. Houghton Inlier forms part of its basement. ||||||
31369|Adelaide Rift Complex|63022|6|Mentioned|p1015|||Includes the Burra Group. ||||||
31369|Adelaide Rift Complex|64400|6|Mentioned|p4|||Probably more a structural term in this context. Includes the Burra, Umberatana and Wilpena Groups.||||||07-FEB-11
31369|Adelaide Rift Complex|67912|6|Mentioned|p13|||Contains the Acraman impact ejecta layer; a widespread, precise marker bed.||||||
31369|Adelaide Rift Complex|68241|6|Mentioned|p29||||||Includes the Nuccaleena Formation.|||
31369|Adelaide Rift Complex|68315|6|Mentioned|p772-773|Neoproterozoic|Neoproterozoic|Sedimentation associated with this Complex is suggested to account for pre-Delamerian Orogeny burial in the Curnamona Province.||||||
31369|Adelaide Rift Complex|69017|6|Mentioned|p96|Cambrian|Neoproterozoic|Part of an extended continental margin E of the Stuart Shelf. 7-12km thick sedimentary package.||||||
31369|Adelaide Rift Complex|69999|5|Briefly described|p5|Neoproterozoic|Neoproterozoic|Represents continental rift to passive continental margin development during break-up of Rodinia (between 850 and 520 Ma). Deformed  and underwent low-grade metamorphism c.520-490 Ma.||||||
31369|Adelaide Rift Complex|70000|5|Briefly described|p30, p39-40|Cambrian|Neoproterozoic|An epicontinental, glacigenic rift basin to stable shelf sequence during Rodinian break-up. Deposition was terminated by the Delamerian Orogeny (c.514-500 Ma).|||Includes Poolamacca Group.|||
31369|Adelaide Rift Complex|70125|5|Briefly described|p399-400|Ediacaran|Ediacaran|A sedimentary succession. Ruled out as a potential distal provenance of detrital zircons in SE Australian beach sand.||||||
31369|Adelaide Rift Complex|70416|6|Mentioned|p63|||Formerly the Adelaide Geosyncline.||||||
31369|Adelaide Rift Complex|71250|6|Mentioned|p69|Middle Cambrian|Neoproterozoic|A N-S oriented fold belt in central South Australia.||||||
31369|Adelaide Rift Complex|71288|6|Mentioned|p134|||Mentioned in the context of the timing of Australia-Laurentia beakup. Presented as Adelaidean Rift Complex.||||||
31369|Adelaide Rift Complex|72464|6|Mentioned|p26|||The time of formation of this Complex is noted as broadly coinciding with the alteration age (c.930-770 Ma) of K-feldspar in a dacite of the Gawler Range Volcanics.||||||
31369|Adelaide Rift Complex|73059|6|Mentioned|p1059, 1061|||Formed from ~800 Ma onwards. A marked change in provenance occurred at ~545 Ma.|||Bonney Sandstone.|||
31369|Adelaide Rift Complex|73302|6|Mentioned|p33|||||||||
31369|Adelaide Rift Complex|73516|6|Mentioned|p2|Cambrian|Neoproterozoic|Deposition terminated by Delamerian Orogeny.||||||
75103|Adelaide Sandstone|64769|6|Mentioned|p28|||Is the name of dimension stone mined from the Hallett Cove Limestone. SA.||||||15-APR-09
28318|Adelaidean Group|22643|6|Mentioned|p191|Early Cambrian|Early Cambrian|||||||
28318|Adelaidean Group|23818|6|Mentioned|p98|Cambrian|Cambrian|Overlying unit: Kanmantoo Group.||||||
28318|Adelaidean Group|34941|6|Mentioned|p234|||||||||
28318|Adelaidean Group|42788|5|Briefly described|p147|||||||||
28318|Adelaidean Group|70840|5|Briefly described|p444-445|Neoproterozoic|Neoproterozoic|Geological province: Delamerian Orogen. Comparable detrital zircon age spectra to the northern Victoria Land Neoproterozoic-early paleozoic metasedimentary rocks. Dominated by cratonic detrital zircon ages (1500-2000 Ma), with a peak at ca. 1700 Ma, and a smaller Grenville-age component increasing towards younger strata. Cratonic component is probably the Gawler craton to the west (Ireland et al., 1998).||||||
83686|Adelaidean Supergroup|73430|6|Mentioned|p491|Neoproterozoic|Neoproterozoic|Delamerian Orogen. Deformed during middle to late Cambrian.|||Callana Group|||
34203|Adelaidean sequence|22671|6|Mentioned|p832||Neoproterozoic|||||||
34203|Adelaidean sequence|22772|5|Briefly described|p62-63,Table13.1,71|Neoproterozoic III|Cryogenian|||||||
34203|Adelaidean sequence|22858|6|Mentioned|Fig14.8p96|||||||||
34203|Adelaidean sequence|22933|6|Mentioned|Table11.1p5,10|Neoproterozoic III|Cryogenian|||||||
34928|Adelaidean succession|23023|6|Mentioned|p1797|||||||||
67918|Ajax Limestone, lower|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Informal - see Ajax Limestone. Age is Atdabanian.||||||12-JUL-06
67918|Ajax Limestone, lower|44133|6|Mentioned|p22|||||||||
72301|Ajax Limestone, middle|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Informal - see Ajax Limestone. Age is Atdabanian to Botoman.||||||12-JUL-06
67917|Ajax Limestone, upper|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Informal - see Ajax Limestone. Age is Botoman||||||12-JUL-06
67917|Ajax Limestone, upper|44133|5|Briefly described|p24, 25, 26|||||||||
81619|Alballa-Karoo Syenogranite|72344|5|Briefly described|p7, p54|Stenian|Stenian|Coompana Province. Intersected in drillholes CDP003 and CDP005. CA-TIMS date is a preferred magmatic age. Petrography, SHRIMP analyses and geochemistry are discussed for several samples.|1149.48 +/- 0.31 (CA-TIMS)|Koonalda Suite|||Equigranular red-brown micro-syenogranite.|
69594|Alberga Formation|61155|5|Briefly described|p17|Middle Miocene|Early Miocene|Geological region: Oodnadatta area. ||||||
78852|Alberga Limestone Member|66131|6|Mentioned|p245|||Oodnadatta area. See also references to Alberga Limestone (p240, p242 Fig.2, p243, p245), said to be "also regarded as member of the Etadunna Formation".||||||
81756|Alcoonie Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Olary Domain.||Strathearn Group.||||
42406|Alcurra dyke swarm|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mafic. Geological Province: Musgrave Block.||||||22-FEB-05
28276|Aldgate (Rhynie) Sandstone|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
39002|Algebuckina sandstone|23883|6|Mentioned|p134|||Geological Province: Great Australian Superbasin.||||||
34949|Alinya Shale|22900|6|Mentioned|83|||Geol province Waigen Sub-basin||||||
35688|Alinya beds""|23288|6|Mentioned|p125||Neoproterozoic|of Stainton et al (1988). Now Alinya Formation.||||||
69945|Alma Formation|61258|5|Briefly described|p399|Paleoproterozoic|Paleoproterozoic|Of the Thackaringa Group. Age: 1704+/-3Ma (Page et al 2000a,b). Geological Province: Broken Hill-Olary region.||||||07-NOV-08
69945|Alma Formation|72037|5|Briefly described|p862|||Geological province: New England Orogen, Gympie Terrane. Nomenclature of Arnold (1996). Depositional environment: deepwater marine. LA-ICP-MS peak detrital zircon U-Th-Pb ages include 302, 345, 384, 427 and 505 Ma.||Unit of Rammutt Formation|||Pale green, massive or laminated mudstone and siltstone interbedded with fine-grained tuffaceous rocks and hyaloclastites,|
82982|Alpha mudstone|73251|6|Mentioned|p49|||Locally named uppermost mudstone of the Namba Formation (Heathgate Resources 1998, pp. 6-9) [the uppermost mudstone is near the base of the Namba Formation].||||||
35689|Alynia beds|23288|6|Mentioned|p125||Neoproterozoic|of Thomas (1990) and Lindsay et al (1992). Now Alinya Formation.||||||
81677|Amaroo Gneiss""|63102|5|Briefly described|p39|||Nomenclature after Laing (1996b); usage is no longer current. See Ameroo Subsuite and Abminga Subsuite. Deformed and metamorphosed granitoids. Equivalent unit; similar composition and age to Basso Granodiorite (Ashley et al. 1996).|||||Leuco-mesocratic granitic gneiss.|
80482|Amaroo Subsuite|63866|5|Briefly described|p41|||Olary Domain, Curnamona Province. [Misspelling of the Ameroo Subsuite].||Basso Suite||||
79845|Amata Dike Swarm|61733|6|Mentioned|p46|||Mis-spelt Amata Dyke Swarm. Represents plume-related mafic intrusions.|c.0.80 Ga.|||||
78352|Amata Dyke Swarm|67536|6|Mentioned|Map Legend|||Musgrave Block. Mapped with Alcurra Dyke Swarm as MN3.|||||Post-Musgravian mafic dykes; variably magnetic, including reversely magnetised.|
78352|Amata Dyke Swarm|72259|6|Mentioned|p10|Tonian|Tonian|[Written as Amata-Gairdner Dyke Swarm].|ca. 830-825 Ma|||||
40413|Amata Suite|24496|5|Briefly described|p17|||NW trending mafic dykes. Correlated with Gairdner Dyke Swarm of the Gawler Craton. Geological Province: Musgrave Block.||||||
40413|Amata Suite|24604|6|Mentioned|p915|||||||||
40413|Amata Suite|61153|5|Briefly described|p344 Fig. 1|Neoproterozoic|Neoproterozoic|Age: 797+/-48 and 790+/-40Ma. Geological Province: Musgrave Inlier. See also p347 Tb. 1.||||||
40413|Amata Suite|61732|6|Mentioned|p36|||Northwest extension of the Gairdner Dyke Swarm.||||||15-JAN-15
40413|Amata Suite|64831|5|Briefly described|p1130|Neoproterozoic|Neoproterozoic|Age: 797+49Ma and 790+/-40 Ma (Zhao and McCulloch 1993a), but described as 'the ca 800Ma suite'. Geological province: Musgrave Province. Comprises mafic dykes referred to, in places, as the Amata Dykes or Amata Suite Dykes.||||||
40413|Amata Suite|65256|6|Mentioned|p17|Cryogenian||Dolerites. Sm-Nd age of 800 Ma (Zhao and McCulloch 1993). Correlated with spilites in Loves Creek Member (Bitter Springs Formation).||||||
40413|Amata Suite|71001|6|Mentioned|p22||||||||Mafic volcanic rocks.|
40413|Amata Suite|71170|5|Briefly described|p146, p150|||See also the Amata Dolerite suite.|||||Mylonitized granitic gneiss and dolerite dykes.|
40413|Amata Suite|72484|5|Briefly described|p23|||Widespread throughout the Musgrave Block. Other age determinations given range from 760 Ma to 797 +/- 49 Ma.|790 +/- 40 Ma.|||Correlated with the Gairdner Dyke Swarm.||
42407|Amata dyke swarm|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Mafic. Geological Province: Musgrave Block.||||||22-FEB-05
42407|Amata dyke swarm|63562|6|Mentioned|p337, p341|||Of Musgrave Inlier. Plume-related magmatism. Other ages are 790 +/- 40 Ma and 797 +/- 49 Ma (Sm-Nd: Zhao et al., 1994).|824+/-4 Ma baddeleyite U-Pb (Glikson et al. 1996)|||||
42407|Amata dyke swarm|69437|5|Briefly described|p22:3|||Of the Gairdner Large Igneous Province.  Intrudes Supersequence 1 in the Officer and Amadeus Basins.|c.825 Ma.|||||12-JUL-16
42407|Amata dyke swarm|69873|6|Mentioned|p73|||Possible equivalent of Tayatea Dyke Swarm in Tasmania.||||||
42407|Amata dyke swarm|72259|6|Mentioned|p1, p9|||[Written as Gairdner-Amata dyke swarm and Gairdner-Amata Dyke (G-A) dyke swarm].||||||
69389|Amata suite|61153|6|Mentioned|p345, p351|||Informal - see Amata Suite. Geological Province: Musgrave Inlier.||||||
29841|Ameroo Gneiss|22884|2|Defined|p40 Fig. 1, p44||Statherian|Correlates with Rasp Ridge Gneiss. Age: 1703+/-6 Ma. Overlain by Weekeroo Fm in parts. Variously described as metagranitoid, massive felsic rock, locally foliated, biotite gneiss, granite gneiss, and adamellite gneiss - essentially a variably fol'd leucoc||||||26-MAR-09
29841|Ameroo Gneiss|23347|5|Briefly described|p55|||Of Laing (1996a). Of the Basso Suite.||||||
29841|Ameroo Gneiss|70657|5|Briefly described|p46|||Laing (1996).|||||Leuco-mesocratic granitic gneiss (deformed and metamorphosed granitoids).|
41668|Ameroo Hill metagranitoid|24197|6|Mentioned|p29|||Informal name. Age: 1703+/-6Ma.||||||07-FEB-11
41668|Ameroo Hill metagranitoid|50605|5|Briefly described|p(i), p1.3, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary Pretectonic A-Type Suite. Age: 1703 +/- 6Ma (Shrimp).||||||07-NOV-08
82097|Anabama granite|72459|6|Mentioned|p68, p90-93|Delamerian|Delamerian|Adelaide Fold Belt.|ca. 500 Ma|||||
82097|Anabama granite|73430|6|Mentioned|p503|||||||||
72302|Andamooka Limestone, lower|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Informal - see Andamooka Limestone.  Age is Tommotian. Geological Province: Arrowie Basin.||||||12-JUL-06
68784|Andamooka Limestone, upper|23981|5|Briefly described|p10 Fig. 5|Early Cambrian|Early Cambrian|Informal - see Andamooka Limestone. Age is Tommotian. Geological Province: Arrowie Basin.||||||
68784|Andamooka Limestone, upper|24507|6|Mentioned|p23|||Informal. See Andamooka Limestone. Contains a ferruginous zone hosting high-grade copper mineralisation.||||||
42419|Angatja Granite Suite|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|See also Angatja Suite. Age: ~1070 Ma. Minor granitoid suite coeval with Giles Complex and Bentley Supergroup.||||||24-JUL-08
42419|Angatja Granite Suite|60683|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Includes the Angatja Granite.||||||20-APR-05
39858|Angatja Suite granite|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Informal name.  Age: 1070Ma.  Geological Province: Musgrave Block.||||||
39858|Angatja Suite granite|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1070 Ma. Massive, weakly magnetic. Geological Province: Musgrave Block.||||||22-FEB-05
78747|Angle Dam Volcanics|70659|2|Defined|Throughout.|Mesoproterozoic|Mesoproterozoic|Named after Angle Dam on Roopena Station. Gawler Craton. Type locality (around 723250 mE, 6373840 mN, GDA 94 zone 53) and reference drillholes details given. Thickness uncertain. Extensional crustal setting. Previously named Angle Dam porphyry (SAMEDAN Oil Corporation of Australia, 1985). Often abbreviated in the text to ADV. Lithology described in detail. Graphic core logs. ||Lower Gawler Range Volcanics.||Overlies Wandearah Formation and Moonabie Formation. Is overlain by Roopena Basalt. Intrudes with peperitic contact or is overlain by Fresh Well Formation.|Porphyritic rhyolite to dacite composed of tabular feldspar phenocrysts, lesser anhedral and embayed quartz phenocrysts and altered biotite phenocrysts in a fine grained groundmass. Porphyritic dacite is strongly fractured or brecciated.|
78747|Angle Dam Volcanics|70816|5|Briefly described|p3-4,17-18|Mesoproterozoic |Mesoproterozoic |Roopena-Myall Creek area, Gawler Ranges. Syn-sedimentary low level volcanic intrusive which has peperitic contacts with the sediments.||Unit of lower Gawler Range Volcanics.||Intrudes lower Fresh Well Formation.|A syn-sedimentary low level volcanic intrusive which has peperitic contacts with the Fresh Well Formation sediments.|
78747|Angle Dam Volcanics|70948|5|Briefly described|p974, 975|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Where exposed along the SE margin of Gawler Ranges, interlayered with Roopena Basalt and Fresh Well Formation.||Unit of lower Gawler Range Volcanics.|||Dacitic and rhyolitic lavas.|
78747|Angle Dam Volcanics|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Mesoproterozoic|Mesoproterozoic|Peperitic contact with Fresh Well Formation.||Gawler Range Volcanics (Lower)||Peperitic contact with Fresh Well Formation.|Rhyolite to dacite, porphyritic, tabular feldspar phenocrysts, lesser quartz and biotite phenocrysts, dark red to purple-red fine-grained groundmass.|
78747|Angle Dam Volcanics|71129|3|Fully described|p35,47,70,73,75-77,184|Calymmian|Calymmian|Geological Province: Gawler Craton. Type locality: area extending from 200m N of Angle Dam to 250m SW of Angle Dam (McAvaney and Wade, 2015b). Reference drillhole: Drillhole SAMEDAN SOC 1 (140474) between 81.15-124.60 m, 723343mE, 6375193mN (McAvaney and Wade, 2015b). Porphyritic rhyolitic to dacitic high level volcanic intrusive with peperitic contacts with the Fresh Well Formation, indicating syn-sedimentary emplacement in shallow subaqueous environments in contact with wet unconsolidated sediment. Thickness, as intersected in boreholes: 14m in FW 6, 43m in SAMEDAM SOC 1, >11m in SAMEDAN SOC 2 and >5m ub SANEDAN SOC 3 where base of Angle Dam volcanics was not penetrated. Occurs in outcrop as a NS-trending linear body ~300m EW and ~900m NS, bound to the west by Angle Dam Fault; shown to extended further west past the Angle Dam Fault (intersected in FW6 ~500m W of ADF) and extends another 1.3km north in the subsurface. Based on interpreted synchronosity with Fresh Well Formation based on field observations, age is constrained to c. 1587 Ma i.e. age of tuff in upper Fresh Well Formation. See also p199,206,225,227,230-231.|c. 1587 Ma|Unit of Gawler Range Volcanics.||Underlain by and intrudes the Moonabie Formation. Overlies the Wandearah Formation. Synchronous with, and interleaved with Roopena Basalt and Fresh Well Formation.|Rhy olite to dacite, porphyritic, tabular feldspar phenocrysts, lesser quartz and biotite phenocrysts, dark red to purple-red fine-grained groundmass.|13-NOV-19
78747|Angle Dam Volcanics|71130|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||Peperitic contact with Fresh Well Formation.|Rhyolite to dacite, porphyritic, tabular feldspar phenocrysts, lesser quartz and biotite phenocrysts, dark red to purple-red fine-grained groundmass.|
78747|Angle Dam Volcanics|71131|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||Peperitic contact with Fresh Well Formation.|Rhyolite to dacite, porphyritic, tabular feldspar phenocrysts, lesser quartz and biotite phenocrysts, dark red to purple-red fine-grained groundmass.|
78747|Angle Dam Volcanics|71414|6|Mentioned|p42 Fig 1|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
78747|Angle Dam Volcanics|72089|4|Described|p2-p4, p15-p16, p19, p21-p22, p24|||Gawler Craton. Only known from outcrop and drilling to the south of Roopena Homestead. Up to 43m thick.||Gawler Range Volcanics, lower||Intercalated with the Roopena Basalt. Intrudes the Fresh Well Formation.|Massive feldspar and minor quartz- and biotite-phyric dacite/rhyolite.|
78747|Angle Dam Volcanics|72090|6|Mentioned|p12, p14|||Gawler Craton.||Gawler Range Volcanics, Lower||||
78747|Angle Dam Volcanics|73110|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||Lower Gawler Range Volcanics.||||
80112|Angle Dam porphyry|68158|5|Briefly described|p4|||Local name; possibly Gawler Range Volcanics.||||Intrudes Moonabie Formation and ?Wandearah Metasiltstone.|Brecciated rhyolite with abundant feldspar, quartz and mica phenocrysts.|
80112|Angle Dam porphyry|73110|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Local name.|||||Rhyolite with abundant feldspar, quartz and mica phenocrysts.|
34318|Angle Dam porphyry""|22629|6|Mentioned|p152|Statherian|Statherian|||||||
41669|Antro Tonalite""|50605|6|Mentioned|p11.1|||||||||
26292|Apamurra Member|23282|6|Mentioned|p77,78|||of Benbow (1982) and originally member of Mount Johns Conglomerate. Now raised to formation and Mt Johns C demoted.||||||
26292|Apamurra Member|38329|2|Defined|p203|Cambrian|Cambrian|||||||
26292|Apamurra Member|40945|6|Mentioned|Fig.3|||||||||
26292|Apamurra Member|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
26292|Apamurra Member|43732|6|Mentioned|Fig.4,p5||Early Cambrian|||||||
26292|Apamurra Member|44109|5|Briefly described|p22 Fig. 20|Cambrian|Cambrian|Of Mount Johns Conglomerate (Marla Group). Geological Province: central Officer Basin.||||||
68904|Archaeocyatha Limestone|24138|5|Briefly described|p10 Fig. 1.1|Cambrian|Cambrian|Refers to the Wilkawillina Limestone. Contains archaeocyatha fossils. Geological Province: Adelaide Geosyncline||||||
77154|Arckaringa Palaeosol|68003|6|Mentioned|p74.|||Of Firman (1988). A thick weathered profile. ||||||
77154|Arckaringa Palaeosol|69023|5|Briefly described|p110|Paleogene|Late Cretaceous|(Firman, 1981). Describes bleaching developed in Bulldog Shale. Also called Stuart Pedoderm (Jessup and Norris, 1971).||||||
77655|Arcoeillina Sandstone|67921|5|Briefly described|Map legend|Cambrian|Cambrian|[Mis-spelling of Arcoeillinna]. Grouped with Wirrildar beds and Observatory Hill Formation. Group description: Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.||||Grouped with Observatory Hill Formation, Wirrildar beds||
77655|Arcoeillina Sandstone|73100|5|Briefly described|Map legend|Cambrian|Cambrian|Subsurface. Mapped as one unit with Wirrildar beds and Observatory Hill Formation.||||||
77655|Arcoeillina Sandstone|73111|5|Briefly described|Map legend.|Cambrian|Cambrian|Mapped as one unit with Wirrildar beds and Observatory Hill Formation. Subcrop and minor outcrop.|||||Fluvial, lacustrine, aeolian and sabkha deposits including micaceous and feldspathic sandstone and mudstone, cherty (Magadi-type) siltstone and carbonate interbeds.|
75615|Arcoeillinna Member|65313|5|Briefly described|p578 Fig. 6|Cambrian|Cambrian|Officer Basin.||Uppermost member of Observatory Hill Formation.||Overlies Oolarinna Member, underlies Apamurra Formation.||26-MAR-12
34535|Arcoelillinna Sandstone|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|Misspelling of Arcoeillinna Sandstone||||||
82210|Arcoelinna Sandstone|72478|6|Mentioned|p11, p51 (App 1, p8), 69|||Officer Basin. See also Arcoeillinna Sandstone p8.||||Shown as overlying Observatory Hill Beds. Overlain by Apamurra Formation.||29-MAR-21
82976|Arcoona Quartzite''|73227|6|Mentioned|p25|||[Written as 'Arcoona Quartzite']. Woomera area.||Wilpena Group||Underlain by Corraberra Sandstone Member. Equivalent to Simmens Quartzite Member.||
67989|Arcoota Beds|44133|5|Briefly described|p190 Fig. 10.29|Early Pliocene|Late Paleocene|Geological Province: Waite Basin.||||||
67989|Arcoota Beds|66131|6|Mentioned|p242 Fig.2|Miocene|Paleocene|Late Paleocene to Late Miocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||||
68746|Ardrossan Clay|60958|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Correlates to Hindmarsh Clay.||||||
26351|Ardrossan Clay and Sandrock|40217|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
26351|Ardrossan Clay and Sandrock|61121|6|Mentioned|Map legend|Pleistocene|Pleistocene|Mentioned in conjunction with Hindmarsh Clay (as equivalent?).||||||
26351|Ardrossan Clay and Sandrock|73107|5|Briefly described|Map legend.|Pleistocene|Pleistocene|||||Equivalent to Hindmarsh Clay.||
76910|Ardrossan Clays|65375|6|Mentioned|p39.|||Used in Wilson (1991). Other superseded names include Ardrossan Soil (e.g. Daily et al. 1976); Ardrossan Clays and Sandrock (Tepper 1879). All replaced by Hindmarsh Clay.||||||
28178|Ardrossan Clays and Sandrock|30825|6|Mentioned|p32|||||||||
28178|Ardrossan Clays and Sandrock|42732|5|Briefly described|map legend|Pleistocene||||||||
28178|Ardrossan Clays and Sandrock|44691|4|Described|map legend||Pleistocene|(I/53-12).||||||
28178|Ardrossan Clays and Sandrock|65375|6|Mentioned|p9, p38. |Pleistocene|Pleistocene|Informal name proposed in first research paper on Yorke Peninsula; equivalent to Hindmarsh Clay. Not in use.||||||
69390|Areyonga Tillites|61153|5|Briefly described|p344-345 Fig. 1|||See also Areyonga tillites. Geological Province: Amadeus Basin.||||||
69391|Areyonga tillites|61153|5|Briefly described|p344-345 Fig. 1|||Informal - see Areyonga Tillites. Overlies Bitter Springs Formation. Geological Province: Amadeus Basin.||||||29-JUN-05
29822|Aristarchus Peridotite|24472|5|Briefly described|p5 Tb.1|Archean|Archean|Geological Province: Harris Greenstone Domain, Gawler Craton. Parent: Mulgathing Complex.||||||07-NOV-08
29822|Aristarchus Peridotite|43052|4|Described|p43, Table 3.2|||Of Mulgathing Complex||||||
29822|Aristarchus Peridotite|50605|5|Briefly described|p8.7|||Of the Mulgathering Complex. Geological Province: Gawler Craton & Curnamona Province.||||||
29822|Aristarchus Peridotite|65376|6|Mentioned|p190.|||||Unit in Mulgathing Complex.||||
29822|Aristarchus Peridotite|68128|6|Mentioned|p2, p84, p97|Palaeoproterozoic|Archaean|Gawler Craton. Informal name. Ultramafic intrusions into this unit bore traces of Ni-Cu sulphide mineralisation.|2488 +/- 9 Ma (SHRIMP U-Pb, magmatic age)|Mulgathing Complex|||Metagabbro.|
29822|Aristarchus Peridotite|73230|5|Briefly described|p10, p14, p16|||Superseded by Aristarchus Metaperidotite and Burden Metagabbro. Previously interpreted as a layered mafic intrusion but mafic-ultramafic lithologies are now known to be different ages and so this interpretation is no longer valid.||||||
24165|Arkaba Hill Beds|36245|2|Defined|p5|Adelaidean|early Adelaidean|Certainly Early Adelaidean and most probably Willouran||||||
24165|Arkaba Hill Beds|37326|6|Mentioned|p3|||||||||
24165|Arkaba Hill Beds|37854|6|Mentioned|p12|||See also P13.||||||
24165|Arkaba Hill Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24165|Arkaba Hill Beds|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24165|Arkaba Hill Beds|40225|3|Fully described|Map sheet|||||||||
24165|Arkaba Hill Beds|40294|3|Fully described|p20|||||||||
24165|Arkaba Hill Beds|41403|5|Briefly described|p67|||||||||
24165|Arkaba Hill Beds|42222|6|Mentioned|Table 1 P5|||||||||
24165|Arkaba Hill Beds|42882|5|Briefly described|p4|||of Callanna Group||||||
24165|Arkaba Hill Beds|43052|5|Briefly described|p175|||of Curdimurka Subgroup.||||||
24165|Arkaba Hill Beds|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup. Laminated stromatolitic dolomite and limestone; interbedded micaceous siltstone, fine sandstone.||||||
24165|Arkaba Hill Beds|72492|5|Briefly described|p2 Fig.1, p2|Neoproterozoic|Neoproterozoic|In the Worumba Anticline.||Curdimurka Subgroup||Overlies Niggly Gap Beds and underlies Kirwan Sandstone. Possibly correlated with  Cooranna Formation.|Includes stromatolites with desiccation cracks and ripples.|
24165|Arkaba Hill Beds|73222|6|Mentioned|p7|Tonian|Tonian|Flinders Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Unconformably underlain by Niggly Gap Beds. Overlain by Kirwan Siltstone. Equivalent to Cooranna Formation and Hogan Dolomite.||
24666|Arkaroola Series""|30177|6|Mentioned|p47|||||||||
24666|Arkaroola Series""|37854|6|Mentioned|p8|||||||||
24666|Arkaroola Series""|41404|6|Mentioned|p86|||||||||
40454|Arkaroola waterhole pegmatite|24593|6|Mentioned|p628|||Informal name.||||||
72303|Aroona Creek limestone|23981|6|Mentioned|p23|||Informal - see Aroona Creek Limestone.||||||
82098|Arthurton granite|72459|6|Mentioned|p51|Mesoproterozoic|Mesoproterozoic||1583 +/- 7 Ma|||||
30347|Artipena Dolomite Member|22510|5|Briefly described|table1p37|||Of the Enorama Shale.  Age: Marinoan. Central Flinders Ranges||||||13-MAR-14
30347|Artipena Dolomite Member|23211|6|Mentioned|p45|||Interpreted to be of deep water origin in Umberatana and Wilpena Groups.||||||
30347|Artipena Dolomite Member|70407|4|Described|p103 Fig 2, p113|Neoproterozoic|Neoproterozoic|Age: Marinoan. Type section designated 2 km south of Artipena Hut.||Of Enorama Shale. |||Two thin dolostones, separated by  3 m of greyish red shale in type section.|
72304|Arumbera Sandstone, lower|23981|5|Briefly described|p10 Fig. 5|Precambrian|Precambrian|Informal name. Geological Province: Amadeus Basin.||||||
72304|Arumbera Sandstone, lower|68270|5|Briefly described|p683|Ediacaran|Ediacaran|Amadeus Basin.||||Underlain by Julie Formation.||
72305|Arumbera Sandstone, upper|23981|5|Briefly described|p10 Fig. 5|Tommotian|Tommotian|Informal name. Geological Province: Amadeus Basin.||||||12-JUL-06
69581|Auburn Bluestone|61237|6|Mentioned|p36|||Commercial term for historic building stone from the mid-north of South Australia state.||||||
27955|Auburn Dolomite|22889|4|Described|p35|Adelaidean|Adelaidean|Auburn Dolomite is superseded by Auburn Dolomite Member as the unit has been down graded from formation to member status, for details of change see p35.||||||
27955|Auburn Dolomite|23818|4|Described|p60|Neoproterozoic|Neoproterozoic|Max. thickness: 5000 ft. Underlain by Undalya Quartzite. Overlain by Saddleworth Formation.||||||05-AUG-08
27955|Auburn Dolomite|29696|6|Mentioned|p2|||||||||
27955|Auburn Dolomite|29780|4|Described|p26|||||||||
27955|Auburn Dolomite|30782|6|Mentioned|p70|||Stratigraphy||||||
27955|Auburn Dolomite|30801|6|Mentioned|p5|||See also P6.||||||
27955|Auburn Dolomite|30802|5|Briefly described|Table 1|||On P7||||||
27955|Auburn Dolomite|30807|6|Mentioned|p103|||Suggested map symbol||||||
27955|Auburn Dolomite|32720|6|Mentioned|Table 1|||||||||
27955|Auburn Dolomite|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean||||||
27955|Auburn Dolomite|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
27955|Auburn Dolomite|32725|6|Mentioned|p6|||Geological map.||||||
27955|Auburn Dolomite|33474|6|Mentioned|Fig.2|||||||||
27955|Auburn Dolomite|33956|4|Described|p1040|||||||||
27955|Auburn Dolomite|34535|5|Briefly described|p60|||Marine||||||
27955|Auburn Dolomite|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27955|Auburn Dolomite|34587|5|Briefly described|p36|||||||||
27955|Auburn Dolomite|34718|6|Mentioned|p13|||||||||
27955|Auburn Dolomite|35270|6|Mentioned|Fig.3|||||||||
27955|Auburn Dolomite|36623|6|Mentioned|Fig.1|||||||||
27955|Auburn Dolomite|36733|6|Mentioned|Table 5|||||||||
27955|Auburn Dolomite|37371|6|Mentioned|p382|||See also P377||||||
27955|Auburn Dolomite|37461|6|Mentioned|Table 5.I|||||||||
27955|Auburn Dolomite|38157|6|Mentioned|Table III|||||||||
27955|Auburn Dolomite|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27955|Auburn Dolomite|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27955|Auburn Dolomite|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27955|Auburn Dolomite|40225|6|Mentioned|Map sheet|||||||||
27955|Auburn Dolomite|40294|3|Fully described|p40|||||||||
27955|Auburn Dolomite|41404|3|Fully described|p110|||||||||
27955|Auburn Dolomite|41405|6|Mentioned|Fig.50|||||||||
27955|Auburn Dolomite|42098|6|Mentioned|p53|||||||||
27955|Auburn Dolomite|42222|5|Briefly described|p14|||||||||
27955|Auburn Dolomite|42720|5|Briefly described|map legend|Torrensian||||||||
27955|Auburn Dolomite|42733|6|Mentioned|map legend|Adelaidean||||||||
27955|Auburn Dolomite|42813|5|Briefly described|p16|||of Burra Group||||||
27955|Auburn Dolomite|43052|5|Briefly described|p181,Table 6.1|||of Burra Group||||||
27955|Auburn Dolomite|43742|6|Mentioned|p40|||||||||
27955|Auburn Dolomite|44659|5|Briefly described|map legend|||Torrensian, lithology.||||||
27955|Auburn Dolomite|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Torrensian.||||||
27955|Auburn Dolomite|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group. Dolomitic siltstone, fine grained sandstone, dark grey dolomite.||||||
27955|Auburn Dolomite|64796|6|Mentioned|p191 Fig.9, p196 Tb.4, p200 Fig.10, p202|Neoproterozoic|Neoproterozoic|Appears in Fig.9 without the lithology/rank.||||Overlies Undalya Quartzite. Is overlain by Saddleworth Formation.||
27955|Auburn Dolomite|66109|6|Mentioned|p200|Proterozoic|Proterozoic||~750 Ma.|||||
27955|Auburn Dolomite|68207|6|Mentioned|p766|||Mentioned in a graph showing Raman spectra of kerogen comprising Precambrian permineralised microfossils; demonstrating they are not merely graphite.|720 Ma.||||Contains Precambrian microfossils in chert.|
27955|Auburn Dolomite|71237|14|Not recorded|p9, 17|||||||||
27955|Auburn Dolomite|71240|2|Defined|p6-7, p9, p17||||||Includes Watervale Sandstone Member.|||
81830|Augen Orthogneiss|68131|6|Mentioned|p13|||Zang (2002). Regrettably capitalised here, implying a formal status which was absent in the first reference. Equivalent to the Wanna Megacrystic Granite Gneiss (Schwartz, 2003), and dated samples from the Gleesons Landing Granite of the Donington Suite.||||||02-MAR-20
38351|Augen orthogneiss|23803|5|Briefly described|p29 Fig. 2|Paleoproterozoic|Paleoproterozoic|Informal.  Age: ~1850Ma. Geological Province: Gawler Craton.||||||07-NOV-08
38351|Augen orthogneiss|60958|6|Mentioned|Map Legend|Paleoproterozoic|Paleoproterozoic|informal name.||||||07-NOV-08
81699|Augusta Shale''|71129|4|Described|p107,110-111,114,116,126,208|Cryogenian|Cryogenian|Of Stuart Shelf. Also referred to as Augusta Shale Member on p111,126. Restricted to eastern Stuart Shelf. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation. Transgressive-regressive siliciclastic sequence, informally named by exploration geologists working in the SIX MILL HILL area.||Unit of Upalinna Subgroup.||Overlain by 'Yudnapinna Beds', or unconformably by Whyalla Sandstone. Underlain by Tapley Hill Formation. Equivalent to Angepena Formation.||22-NOV-19
81624|Augusta shale''|70334|6|Mentioned|p20,38,51|||Geological province: Gawler Craton. Of Stuart Shelf. Informal term used by exploration companies on the Stuart Shelf; equivalent to Angepena Formation (Mason 1979).||||||
81624|Augusta shale''|72247|6|Mentioned|p41|Neoproterozoic|Neoproterozoic|Of Mason (1978). Of Stuart Shelf.||||||16-SEP-19
29911|Ayres Range Swarm""|43052|6|Mentioned|p165|||Synonym for Alcurra Dyke Swarm||||||
81757|Babbage Volcanics|67323|5|Briefly described|p37|||Throughout the Mount Painter and Mount Babbage Inliers, northern Gawler Craton. Accompanied by emplacement of A- and I-type granites; this magmatism forms part of a hotspot track along the eastern edge of Proterozoic Australia.|~1575-1555 Ma.|||||
27322|Backy Point Beds|35255|5|Briefly described|p9|||See als Figs.4 & 6.||||||
27322|Backy Point Beds|35270|4|Described|p5|||||||||
27322|Backy Point Beds|35565|6|Mentioned|p21|||Mapping and stratigraphy||||||
27322|Backy Point Beds|35678|6|Mentioned|Fig.2|||Geological cross-sections, northern Yorke Peninsula.||||||
27322|Backy Point Beds|35706|6|Mentioned|Fig.1|||||||||
27322|Backy Point Beds|36507|6|Mentioned|p116|||||||||
27322|Backy Point Beds|37461|6|Mentioned|Table 5.I|||||||||
27322|Backy Point Beds|38581|6|Mentioned|Fig.2|||||||||
27322|Backy Point Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27322|Backy Point Beds|39349|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27322|Backy Point Beds|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
27322|Backy Point Beds|39724|6|Mentioned|Fig.6|||||||||
27322|Backy Point Beds|39762|6|Mentioned|Table 1|||||||||
27322|Backy Point Beds|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27322|Backy Point Beds|39866|5|Briefly described|p267|||||||||
27322|Backy Point Beds|40448|6|Mentioned|p37|||||||||
27322|Backy Point Beds|41402|6|Mentioned|p36|||||||||
27322|Backy Point Beds|41403|4|Described|p49|||||||||
27322|Backy Point Beds|41667|6|Mentioned|p6|||||||||
27322|Backy Point Beds|42088|5|Briefly described|p544|||See also Fig.2 P546||||||
27322|Backy Point Beds|42235|5|Briefly described|p134|||||||||
27322|Backy Point Beds|44934|5|Briefly described|Map Legend||Adelaidean|||||||
27322|Backy Point Beds|69666|6|Mentioned|p26|||Mason, Thomson and Tonkin (1978). Sediments associated with Beda Volcanics. Briefly defined as Backy Point Formation by Crawford and Forbes (1969).||||||
27322|Backy Point Beds|71895|6|Mentioned|p23|||See also Backy Point Formation.||||||
75014|Bailey Range Siltstone Member|64455|5|Briefly described|p138 Fig. 1|Ediacaran|Ediacaran|Of Brachina Formation. Underlain by Moorillah Siltstone Member. Glauconitic sandstone.||||||29-JAN-09
37133|Balcanoona formation|23562|6|Mentioned|p295|||Superseded by Balcanoona Formation.||||||
67919|Balcoracana Formation, upper|44133|6|Mentioned|p30|Middle Cambrian|Middle Cambrian|||||||
31913|Balcorana formation|43876|14|Not recorded|p549||Middle Cambrian|||||||
81698|Bald Member''|71129|6|Mentioned|p116|||Of Stuart Shelf. Superseded; see Brighton Limestone. Previously considered part of the underlying Tapley Hill Formation by Australian Selection exploration geologists.||||||22-NOV-19
75851|Bald Rock Beds|6111|6|Mentioned|p23 Fig.1.|Early Cambrian||||||||17-SEP-12
75851|Bald Rock Beds|62785|6|Mentioned|p44 Fig.1|Early Palaeozoic|Early Palaeozoic|North coast Kangaroo Island. ?Middle Cambrian.||||||20-MAR-12
75851|Bald Rock Beds|65667|6|Mentioned|p1222 Fig.1|Middle Cambrian|Middle Cambrian|Overlies Boxing Bay Formation. Age shown as ?middle Cambrian.||||||10-DEC-12
75851|Bald Rock Beds|65892|6|Mentioned|p22 Fig.10.|Middle Cambrian|Middle Cambrian|North coast of Kangaroo Island.||||||
75851|Bald Rock Beds|67344|6|Mentioned|p260 Fig.1|Cambrian|Cambrian|Middle Cambrian age.||||||
75851|Bald Rock Beds|75071|6|Mentioned|p213|Cambrian|Cambrian|Kangaroo Island.||||||
34790|Bald Rock beds""|22766|5|Briefly described|Fig.2 p561, p563|Ordovician||||||||
81668|Bald member''|70334|5|Briefly described|p20 fig 11, p38,50|||Geological province: Gawler Craton. Of Stuart Shelf. Informal term used by exploration companies on the Stuart Shelf (Mason 1979). Previously considered part of underlying Tapley Hill Formation.||Unit of Brighton Limestone.||||22-NOV-19
34005|Balqhidder Formation|22581|5|Briefly described|Fig.2,p37|||Kanmantoo Group, Kanmantoo Basin. Overlies Tunkalilla Formation. Overlain by Petrel Cove Formation||||||07-MAR-16
72306|Balquhidder formation|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Informal name. of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||
83059|Balquihidder Formation|73188|6|Mentioned|p316|Early Cambrian|Early Cambrian|[Possibly a misspelling of Balquhidder Formation]. Mount Lofty Ranges.||Bollaparudda Subgroup, Kanmantoo Group|||Medium-grained turbidites.|
40397|Balta Granite Suite|24422|5|Briefly described|p86|Mesoproterozoic|Mesoproterozoic|Age: 1584 +/- 18 Ma (U-Pb). Geological Province: Mount Woods Inlier, Gawler Craton. See also - Balta Granitic Suite.||||||
40397|Balta Granite Suite|67621|6|Mentioned|p211, 222-224|||Intrudes the Mount Woods Inlier.|1584 +/- 18 Ma (Ambrose and Flint, 1981).|||||
40397|Balta Granite Suite|72949|6|Mentioned|p36|Calymmian|Statherian|Mount Woods Inlier. A-type (alkali-calcic) granite.|1584 +/- 18 Ma|||||
40397|Balta Granite Suite|73155|6|Mentioned|p266, p282 Fig.13, p283|Calymmian|Calymmian|Mount Woods Domain. See also Balta Suite, Balta Granite.|ca. 1584 Ma|Mount Woods Complex, Hiltaba Suite||||
40397|Balta Granite Suite|73165|6|Mentioned|p637, Fig. 12|Calymmian|Calymmian|Gawler Craton, Mount Woods Inlier.|ca 1584 Ma|||||
40398|Balta Granitic Suite|24422|5|Briefly described|p86 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ca. 1585 Ma. Geological Province: Mount Woods Inlier, Gawler Craton. See also - Balta Granite Suite.||||||
69926|Balta Suite|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic|Mesoproterozoic|Age: <1600Ma. Geological Province: northern Gawler Craton.||||||
69926|Balta Suite|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
69926|Balta Suite|73155|6|Mentioned|p283 Fig.14|||See also Balta Granite, Balta Granite Suite.||Hiltaba Suite||||
76824|Banda Siltstone|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|SE Flinders Ranges.||||Underlies the Wilyerpa Formation, probably unconformably; overlies the Pualco Tillite.||26-APR-12
32471|Banded Marl Member|23818|5|Briefly described|p191|Late Eocene|Late Eocene|Of the Blanche Point Marls. Crowded with the gastropod Turritella aldingae Tate.||||||
32471|Banded Marl Member|33330|14|Not recorded|p171|||||||||
32471|Banded Marl Member|34308|6|Mentioned|p191|||Middle member of Blanche Point Marls.||||||
28352|Basal Dolomite Member|42723|5|Briefly described|map legend|Sturtian||of Tapley Hill Formation.  Not intended as a formal name?||||||
34660|Basket Range Sandstone""|22869|6|Mentioned|P38|||Now part of the Mundallio Subgroup||||||
35894|Basso Granodiorite|23347|6|Mentioned|p55|||Formerly regarded as a metagranite of Benton (1994).  Superseded by Ameroo Subsuite.||||||24-MAR-09
35894|Basso Granodiorite|70657|5|Briefly described|p46|||Benton (1994).|||||Leuco-mesocratic granitic gneiss (deformed and metamorphosed granitoids).|
81678|Basso Granodiorite""|63102|5|Briefly described|p39|||Nomenclature after Benton (1994); usage no longer current. See Ameroo Subsuite and Abminga Subsuite (terms formalised by Conor 2000b). Deformed and metamorphosed granitoids. Equivalent unit; similar composition and age to Amaroo Gneiss (Ashlet et al. 1996).|||||Leuco-mesocratic granitic gneiss.|
32797|Batesfordian Stage|44238|14|Not recorded|Fig.3||Miocene|||||||
23369|Beanbush beds|13497|6|Mentioned|p114|||Informal name (Price et al., 1985) that was replaced by the Cuddapan Formation by Channon and Wood (1989). ||||||
23369|Beanbush beds|41288|6|Mentioned|p159|Late Triassic|Late Triassic|Top of Cooper Basin. PT5. Shown as unconformably between Morney Beds below and Poolowanna Fm, Eromanga Basin, above. Shown as Beanbush Beds p158 Fig.7.||||||09-APR-15
27333|Beaumont (Auburn) Dolomite|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
80465|Belair "Group"|71529|14|Not recorded|p2 |||||||||
80333|Belair Group|71237|14|Not recorded|p7, 9|||||||||
37127|Belair Sub Group|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|Informal||||||
37127|Belair Sub Group|23869|5|Briefly described|p22 Fig. 4|||Informal - see Belair Subgroup.||||||
41549|Belair Subgroup Formation|50615|5|Briefly described|p303, Fig. 2.|||Misspelt? Probobly intended to be Belair Subgroup. Includes the Mitcham quartzite. Geological Province: Adelaide Fold Belt.||||||
39213|Belair Subgroup Shale|23731|6|Mentioned|p27|||Informal name.||||||
40992|Belfast formation|24562|6|Mentioned|p78|||Informal.  See Belfast Formation.||||||20-MAY-04
67920|Beltana Dolomite""|44133|6|Mentioned|p22|||Hull, 1973. informal name||||||
67920|Beltana Dolomite""|71628|6|Mentioned|p19: 145|||Informal South Australian unit.||||||
40455|Beltana willemite|24593|6|Mentioned|p629|||Informal name.  Age: ca.435Ma (K-Ar, Groves et al, 2003).||||||
40455|Beltana willemite|44133|6|Mentioned|p25|||Orebodies. Horn, 1975.||||||
82026|Benagerie Ridge Diorite|72454|5|Briefly described|p21 Tb.2|Calymmian|Calymmian|Benagerie Ridge, Curnamona Province. May be sample description rather than stratigraphic unit name. Part of the Mudguard Domain. Age determined by SHRIMP method Fanning (1997).|1585 -/+ 195 Ma.|||Overlies Willyama Supergroup.|Includes quartz-biotite diorite.|
76911|Benagerie Ridge Volcanics|65375|6|Mentioned|p13.|||||||||
76911|Benagerie Ridge Volcanics|69255|5|Briefly described|p788|Calymmian|Calymmian|Curnamona Province.|c.1585 Ma.|||Correlated with Gawler Range Volcanics.|Contains mafic units.|
76911|Benagerie Ridge Volcanics|70659|5|Briefly described|p47||||1591 +/- 6 Ma max depositional age||||Sandstone and siltstone with lesser mudstone interlayered with basaltic lavas.|09-FEB-17
76911|Benagerie Ridge Volcanics|72462|6|Mentioned|p7|||A-type.|ca 1590-1570 Ma|||||
76911|Benagerie Ridge Volcanics|72949|6|Mentioned|p36, p38|Calymmian|Calymmian|Curnamona Province. Broken Hill / Olary Blocks.|1587-1584 Ma|||||
76911|Benagerie Ridge Volcanics|73155|6|Mentioned|p264|||Curnamona Province, central-western.|||||Lower grade, upper crustal rocks.|
76911|Benagerie Ridge Volcanics|73524|6|Mentioned|p4, p20|Calymmian|Calymmian|Curnamona Province. Correlative of Gawler Range Volcanics.|c. 1600-1570 Ma|||||
81940|Benagerie volcanics|72461|6|Mentioned|p6||||1590-1580 Ma|||||
24712|Bendieuta Formation|23981|5|Briefly described|p8-9 Fig. 4|Early Cambrian|Early Cambrian|Age is Botoman. Geological Province: Arrowie Basin.||||||04-FEB-08
24712|Bendieuta Formation|42458|5|Briefly described|Fig.2 p699|||||||||01-NOV-18
24712|Bendieuta Formation|44133|4|Described|p4 Fig. 7.2, p23, 24|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Disconformably overlies Wilkawillina Limestone. Conformably overlies: lower Mernmerna Formation. Maximum Thickness: 238m.||||||01-NOV-18
24712|Bendieuta Formation|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
24712|Bendieuta Formation|60889|5|Briefly described|p247 Fig.4|Early Cambrian|Early Cambrian|Thickness: 240 m.||Hawker Group||||
24712|Bendieuta Formation|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Planar to trough cross-bedded, coarse-grained, quartz sandstone, ooid-peloid grainstone and fenestral limestone.||||||
24712|Bendieuta Formation|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|||||Shown as lateral equivalent to upper Wilkawillina Limestone in part, Nepabunna Siltstone, Midwerta Shale, Mernmerna Formation (Parara Limestone) in part.||
24712|Bendieuta Formation|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
24712|Bendieuta Formation|65892|6|Mentioned|p9 Fig.4. |Early Cambrian|Early Cambrian|Arrowie Basin.||Unit in Hawker Group.||||
24712|Bendieuta Formation|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|||||||
24712|Bendieuta Formation|68735|6|Mentioned|p235 Fig.3|Early Cambrian|Early Cambrian|||Hawker Group.||||10-APR-17
24712|Bendieuta Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
24712|Bendieuta Formation|71102|5|Briefly described|p242,249,251|||Of Arrowie Basin. Highstand siliciclastic deposits. Intersected section:  LMNB (Lower Mernmerna, North Boundary Creek, Chambers Gorge, E Flinders Ranges).|||||Mssive, fine calc-sandstone to fine sandy limestone. Sandy at base, grading into pelletal limestone.|
24712|Bendieuta Formation|72429|6|Mentioned|p960|Lower Cambrian|Lower Cambrian|Previous name for the Bendieuta Member of the Mernmerna Formation [see entry].||||||
67921|Bendigo"" Granite|44133|5|Briefly described|p56 Table 7.3|Ordovician|Ordovician|Medium grained granodiorite. I-Type. Age: 454 +/- 84Ma, 564 +/- 57Ma.||||||
68298|Bentley Group|24111|6|Mentioned|p209|Mesoproterozoic|Mesoproterozoic|Geological Province: Officer Basin.||||||
80375|Bentley Supergroup, lower|71210|6|Mentioned|p8-p9, p20, p22, p136||||||Includes Kunmarnara Group.|||07-FEB-18
80376|Bentley Supergroup, upper|71210|6|Mentioned|p9-p10, p20||||||Includes Tollu Group.|||07-FEB-18
77425|Beverley Sands|65194|5|Briefly described|p47-48|||Informal? Also called the Beverley Sand unit. From text: [quote] effectively an aquifer confined between the Alpha Mudstone and the Beverley Clay/Willawortina Formation. [end quote] Of Namba Formation, overlain by Beverley Clay. Mature, well-sorted, quartz-rich silty sands; minor clay and organic-rich intraclasts. Hosts uranium mineralisation.||Unit in upper Namba Formation.||||08-APR-16
77425|Beverley Sands|65925|5|Briefly described|p57, p59, p61, p66.|Miocene|Miocene|Permeable sand lenses host uranium mineralisation, mostly near contact with organic-rich Alpha Mudstone.||Unit in Namba Formation.|||Grey silt with quartzose sandstone lenses.|08-APR-16
77425|Beverley Sands|69562|6|Mentioned|p662 Tb.2, p675|||Lenticular; confined between Beverley Clay and Alpha Mudstone. Hosts the Beverley U deposit. Electrical conductivity value used in forward modelling: 100-400 mS/m.||Unit in Namba Formation.||Overlies (incised into) Alpha Mudstone. Is overlain by Beverley Clay.||
82983|Beverley sand|73251|6|Mentioned|p52|||(Heathgate Resources, 1998). Of the 'Beverley sequence'; uppermost sedimentary cycle of Namba Formation. Includes sandstone-hosted uranium mineralisation.||||||
75078|Bewooloo Formation|62993|6|Mentioned|p37, p39|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Ethiudna Subgroup||||19-DEC-21
75078|Bewooloo Formation|64741|5|Briefly described|p301 Fig. 4, p302, p304|Paleoproterozoic|Paleoproterozoic|Base of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain. Fine, silicicalstic metasediments.|||Montstephen Metabasalt Member|||02-AUG-12
75078|Bewooloo Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75078|Bewooloo Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. Appears mis-spelled as Beewooloo Formation (p39) and Beewooloo Member (p37).||Ethiudna Subgroup|Includes the Montstephen Metabasalt Member|Overlies the Tommie Wattie Formation. Overlain by the Peryhumuck Formation.||
75078|Bewooloo Formation|70657|4|Described|p14-15, p20, p22-23, p30, p46, p66|Statherian|Statherian|Northern Walparuta Inlier, Olary Domain, Curnamona Province. Age inferred Tb.1. No equivalent in Broken Hill Domain. Appears as Beewooloo Formation on p14 and p29. Mn-enrichment described.|<1718-1715 Ma|Basal (locally) Ethiudna Subgroup.||Overlies Tommie Wattie and ?Cathedral Rock Formations. Underlies Peryhumuck and ?Toraminga Formations. Interbedded with Montstephen Metabasalt.|Fine-grained psammitic metasediment containing pillow and amygdaloidal metabasalt (Montstephen Metabasalt), volcaniclastic conglomerate, polymict conglomerate, garnet quartzite, and Mn-Fe "exhalite".|
83040|Big Lake Granites|73184|6|Mentioned|p197|Carboniferous|Carboniferous|Cooper Basin. [Misspelling of Big Lake Granite?]|ca 330-300 Ma|||||
83637|Big Lake Granodiorite|73167|6|Mentioned|p662, p664|Carboniferous|Silurian|Emplaced during prolonged period of fault reactivation in the Alice Springs Orogeny between the Silurian and Carboniferous. Uranium-rich. Shown as Big Lake Volcanics p664.||||||
83637|Big Lake Granodiorite|73479|6|Mentioned|p157|Carboniferous|Carboniferous|See also Big Lake Volcanics p156 Fig.2, Moomba-Big Lake Granodiorite p162.||||||
72787|Big Lake Suite granites|63056|5|Briefly described|p80|Carboniferous|Early Carboniferous|Informal - see Big Lake Suite.||||||06-FEB-07
83058|Big Lake Volcanics|73244|6|Mentioned|p86|||[Possibly a variation of Big Lake Suite]. Associated with the Alice Springs Event.||||||
83058|Big Lake Volcanics|73343|6|Mentioned|p337|Devonian|Devonian|||||||
83058|Big Lake Volcanics|73479|6|Mentioned|p156 Fig.2|Carboniferous|Silurian|See also Big Lake Granodiorite p157.||||||
73828|Big Lake granite suite|24546|5|Briefly described|p2 - 6 Tb.1|Paleozoic|Paleozoic|Informal. Emplaced at ~325 Ma. Intrudes Mount Painter Province.||||||07-NOV-08
75990|Big Lake granites|65382|5|Briefly described|p714|Serpukhovian|Serpukhovian|Warburton Basin region. Age of 323 +/- 5 Ma given. See also Big Lake Suite, p717 App2.||||||
80361|Billeroo Alkaline Magmatic Complex|70657|6|Mentioned|p48, p62|||Curnamona Province. Appears as Billeroo Alkaline Igneous Complex on p62.||||||
73627|Billeroo North alkaline magmatic complex|63539|5|Briefly described|p33|||Series of layered feldspathic ijolites (true 'ijolites' are nepheline-pyroxene rocks without modal feldspar), massive syenite bodies (including K-feldspar porphyries) and alkali lamprophyre dykes; extensive brecciated metsedimentaries+minor pegmatite/qtz.||||||20-SEP-07
73627|Billeroo North alkaline magmatic complex|69650|6|Mentioned|p6, p32|||Rutherford et al. (2007). All capitalised on p6. Superseded by Billeroo Intrusive Complex.||||||
81679|Billeroo alkaline magmatic complex''|63102|5|Briefly described|p41,53|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Nomenclature of Bell et al. (1979), Rutherford et al. (2003). Shows evidence of deformation e.g. Clasts of schistose country rock in breccia zones, and metasomatism and contact metamorphism of the host schists (probably Ethiudna Subgroup), suggesting intrusion after main Olarian metamorphic events, however weak foliation infers the complex was likely intruded before the cessation of deformation.  Probably synchronous with a late stage of the Olarian Orogeny.||||Intrudes into Ethiudna Subgroup.|Syenite, ijolite, minor possible carbonatite (calcite and siderite), and breccia.|
73626|Billeroo alkaline magmatics|63539|5|Briefly described|p33|||Geological Province: Olary Domain/Curnamona Province.  Age given as mid-Proterozoic.||||||03-FEB-16
35468|Billeroo metajaspilite|23289|14|Not recorded|p15|||||||||10-SEP-19
40387|Billy Creek Formation shale|24484|6|Mentioned|p806 Fig. 4|||Informal - see also Billy Creek Formation.||||||
67922|Billy Creek Formation, lower|44133|6|Mentioned|p30|||||||||
35556|Billy Creek Limestone|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 4 of Early Cambrian. Unsure of relationship to Billy Creek Formation. Correlate of Andamooka Limestone.||||||
74004|Billy Creek Tuff|61307|5|Briefly described|p14 Fig. 6|Early Cambrian|Early Cambrian|Age: 522.8+/-1.8Ma. ||||||
30093|Bimba Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
30093|Bimba Suite|22960|5|Briefly described|p92||Paleoproterozoic|||||||07-NOV-08
30093|Bimba Suite|23223|5|Briefly described|p39|||Described as 'Bimba suite - Ettlewood Calcsilicate Member (BS-ECM)' - meaning equivalence. of Allendale Metasediments, Broken Hill Group. Broken Hill Domain.||||||
30093|Bimba Suite|23248|5|Briefly described|Fig2p169|||||||||
30093|Bimba Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
30093|Bimba Suite|43086|4|Described|p4|||||||||
30093|Bimba Suite|63102|6|Mentioned|p13, p23|||Geological province: Olary Domain, Curnamona Province. Superseded; Used by Clarke et al (1986) to stratigraphically link Olary Domain stratigraphy to the 'suite' terminology used at the time as the Broken Hill mine sequence.||||||22-OCT-19
30093|Bimba Suite|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Block.||||||07-NOV-08
30093|Bimba Suite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Olary Domain. Informal name.||Unit in Willyama Supergroup.||Overlies Calcsilicate Suite. Is overlain by Pelite Suite.||
30093|Bimba Suite|70657|6|Mentioned|p34|||One of a number of name variations including Bimba Formation, horizon, and Sulphide Member. This name was used by Clarke et al. (1986) to tie the Olary Domain stratigraphy to the suites in the Broken Hill Domain. Subsequently, the name Bimba Formation has become entrenched, and is used in this study; see references (p5, p10 Fig.4, p12, p13 Fig.6, p14-16, p20-21, p24, p28-30, p32-39, p41, p43-44, p58, p60, p63-68, p73-75, p77).||||||
34772|Bimba Suite""|22939|6|Mentioned|p243|||Informal||||||
77426|Bimba Sulfide Member|65925|5|Briefly described|p143 Appendix 2.|||See Bimba Sulphide Member.|||||Ironstone, sulfide-rich; banded iron silicate formation; thin units and lenses of calcsilicate; marble; calc-albitite; plagioclase-rich metasediment in graphitic psammitic-pelitic metasediment.|30-OCT-12
29845|Bimba Sulphide Member|22884|2|Defined|p40 Fig. 1, p45||Paleoproterozoic|Lies within the Weekeroo Formation and Meningie Well Formation. Max.thickness: 100m. Marker unit of sulphide-rich ironstone and banded iron silicate formation - detailed lith. included.||||||26-MAR-09
36993|Bimba formation""|23476|5|Briefly described|p50|||Of Ethiudna Subgroup. Overlying unit: Broken Hill Group.||||||
36993|Bimba formation""|23731|5|Briefly described|p15, p16, p51|||Of Willyama Supergroup.||||||
36993|Bimba formation""|24381|6|Mentioned|p58|||||||||
34822|Bimba suite|22960|5|Briefly described|p90||Paleoproterozoic|Informal Name.  Shallow water transitional carbonate-evaporite mud.||||||10-SEP-19
34822|Bimba suite|23210|6|Mentioned|p26 Fig.1|||||||||
35876|Bimba sulphide member""|23347|6|Mentioned|p51|||Informal name of Laing (1996a) - who restricted the Bimba prefix to sulphidic parts of the "Bimba formation" (as named by Esso, 1979, annual report).||||||05-MAR-13
76912|Bimbowie Suite|65375|6|Mentioned|p13.||||c.1590 Ma.|||||
37955|Bimbowrie Granite|24307|5|Briefly described|p971|Mesoproterozoic|Mesoproterozoic|||||||
37955|Bimbowrie Granite|62514|5|Briefly described|p747 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Bimbowrie Suite. Age: c.1580Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
37955|Bimbowrie Granite|69650|6|Mentioned|p15|||Originally Bimbowrie Granites (Benton, 1994); subsequently Bimbowrie Suite (Conor, 2004).||||||
78689|Bimbowrie Granites|67540|6|Mentioned|p25, 29|||Of Benton (1994). Subsequently Bimbowrie Suite (Wade, 2011).||||||12-MAR-14
78689|Bimbowrie Granites|69650|6|Mentioned|p15|||Benton (1994). Subsequently Bimbowrie Suite (Conor, 2000).||||||
78689|Bimbowrie Granites|70657|5|Briefly described|p48|||Benton (1994), for a widespread set of two-mica granites in the Olary Domain. Modified by Conor (2000) to Bimbowrie Suite. Proposed in this study to restrict this latter name to include the "regional" two-mica S-type granites.||||||
81682|Bimbowrie Granites''|63102|6|Mentioned|p41|||Geological province: Olary Domain, Curnamona Province. Nomenclature of Benton 1994. Renamed by Conor (2000a) as Bimbowrie Suite to conform to general Olary nomenclature, and reclassified as Bimbowrie Supersuite (this study).||||||
69583|Bimbowrie Suite granites|61239|6|Mentioned|p56|||Informal name. Refers to granites within the Bimbowrie Suite. Recrystallisation age: 1596-1573Ma.||||||
69583|Bimbowrie Suite granites|62724|5|Briefly described|p17 Fig. 4|||Informal - see Bombowrie Suite. Includes two-mica S-type granites. Age: ~1590-1580Ma. Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
39299|Bimbowrie Suite""|24289|6|Mentioned|p47|||Informal name.||||||
39299|Bimbowrie Suite""|50081|6|Mentioned|p43|||Informal name. Geological Province: Curnamona Province.||||||24-FEB-05
78690|Bimbowrie Supersuite|63102|4|Described|p38,41-43,47,50-54|Calymmian|Calymmian|Geological province: Olary Domain, Curnamona Province. Voluminous ?syn- to post-orogenic S-type-dominated granites in the Olary Domain, equivalent are the Mundi-Mundi and related granites of the Broken Hill Domain. Locally foliated or cut by shear zones. Shows pervasive and fracture-controlled albitisation (+\-actinolite, titanite). Tentatively includes the 'regional' two-mica S type granites and related minor intermediate rocks, the biotite-granites, alaskites and related intermediate rocks of the Crockers Well-Billeroo region, and the mafic and I-type felsic volcanics and possible intrusives of the Benagerie Ridge. Reported U-Pb zircon ages include 1579+\-2 Ma (Ludwig and Cooper, 1984), 1580 Ma (Cook et al., 1984) and 1590 Ma (Cook 1993, Cook et al 1994). Also includes Rb-Sr muscovite age of 1580+\-32 Ma, which overlaps with major thermal events in the Broken Hill Domain. Temporally equivalent to Hiltaba Suite I-A type granitoids.|~1580 Ma|||Intrudes into Ethiudna Subgroup.|Syenite, ijolite, minor possible carbonatite (calcite and siderite), and breccia.|22-OCT-19
78690|Bimbowrie Supersuite|67540|6|Mentioned|p37|||Of Conor et al (2006). Replaced by Ninnerie Supersuite.||||||12-MAR-14
78690|Bimbowrie Supersuite|69650|6|Mentioned|p1|||Conor et al. (2006).||||||
78690|Bimbowrie Supersuite|70657|5|Briefly described|p48|||Conor (2000); previously the Bimbowrie Granites of Benton (1994). Subsequently the Bimbowrie Supersuite (Conor, 2004). Because these granites are widespread,chemically variable and show varioation in age, these authors propose the new name of Ninnerie Supersuite to include all Mesoproterozoic granites in the region, and the Bimbowrie Supersuite be discontinued.||||||
68090|Bimbowrie suite""|60485|5|Briefly described|p28 Fig. 2|Calymmian|Calymmian|Informal name for an igneous suite within the Olary Domain. Age: 1600-1580 Ma. Geological Province: Olary Domain.||||||28-APR-05
81683|Bimbowrie suite''|63102|6|Mentioned|p13|||Geological province: Olary Domain, Curnamona Province. See Bimbowrie Suite.||||||
81939|Bimbowrie supersuite''|72461|6|Mentioned|p6||||1600-1580 Ma|||||
70564|Birksgate Complex gneiss|61524|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Informal reference to gneiss within the Birksgate Complex. See also Birksgate Gneiss and Birksgate Complex. Geological Province: Musgrave Province.||||||
70565|Birksgate Gneiss|61524|6|Mentioned|p21 (photo)|Mesoproterozoic|Mesoproterozoic|Probably an informal name and refers to the gneiss within the Birksgate Complex.? Layered quartz and K-feldspar. Geological Province: Musgrave Province.||||||
29904|Birksgate Granitic Complex""|43052|6|Mentioned|p156|||||||||
38637|Bitalli Rhyolite|24346|5|Briefly described|p98 Fig.1, p112 App 1|||Of Gawler Range Volcanics.||||||
38637|Bitalli Rhyolite|24356|5|Briefly described|p1594|Mesoproterozoic||Of the lower part of Gawler Range Volcanics.||||||
38637|Bitalli Rhyolite|72065|5|Briefly described|p105|Calymmian|Calymmian|Geological province: Gawler Craton.||Unit of Gawler Range Volcanics.||||
69392|Bitter Springs volcanics|61153|5|Briefly described|p344-345 Fig. 1|||Informal name. Geological Province: Amadeus Basin.||||||
37527|Black Hill Gabbro|23309|6|Mentioned|p29|||||||||
37527|Black Hill Gabbro|23932|5|Briefly described|p680 Fig. 8|Ordovician|Ordovician|Geological Province: Adelaide Fold Belt. Age: ~485 Ma.||||||
40341|Black Hill gabbros|23932|6|Mentioned|p682|||Informal-refers to Black Hill Gabbro.||||||
40174|Black Hills Norite|24599|5|Briefly described|p498|Ordovician|Cambrian|Age: 490-480Ma.  Geological Province: Adelaide Fold Belt.||||||
40174|Black Hills Norite|73118|6|Mentioned|p21|45||Eastern edge of outcrop of Kanmantoo Group rocks in SA.|490 +/- 39 Ma (Rb-Sr: Foden et al., in prep.)|||||
76830|Black Yardea Dacite|67028|5|Briefly described|p362, p364,  Tb.1, p373|Calymmian|Calymmian|Different unit from Yardea Dacite or just different sample site? Information on magnetic characteristics presented. Most intensely magnetic unit sampled. Kokatha-type.||Gawler Range Volcanics||||24-APR-12
24732|Blanche Point Banded Marl Member|30250|6|Mentioned|p2|||||||||
24732|Blanche Point Banded Marl Member|31515|6|Mentioned|p291|||||||||
24732|Blanche Point Banded Marl Member|34295|5|Briefly described|p33|||||||||
24732|Blanche Point Banded Marl Member|35689|6|Mentioned|Fig.4|||Reference Reynolds 1953.||||||
24732|Blanche Point Banded Marl Member|38621|6|Mentioned|Table 1|||Refers Reynolds  1953.||||||
24732|Blanche Point Banded Marl Member|40442|5|Briefly described|Fig.17|||||||||
29460|Blanchetown Formation|42966|5|Briefly described|p406|||Superseded by Blanchetown Clay||||||
40357|Blanchtown clay|23921|5|Briefly described|p1109 Table 1, p1111 Fig. 2e|Quaternary|Quaternary|Geological Province: Murray Basin||||||
34652|Blinman Diapir|22868|6|Mentioned|p34|||||||||
26403|Blowhole Creek Siltstone Member|22643|5|Briefly described|p193, fig6|Early Cambrian|Early Cambrian|Age: Botomian.||||||
26403|Blowhole Creek Siltstone Member|24465|6|Mentioned|p347|Early Cambrian|Early Cambrian|Of Carrickalinga Head Formation. Superseded by Blowhole Creek Member.||||||
26403|Blowhole Creek Siltstone Member|30377|4|Described|p204|||||||||
26403|Blowhole Creek Siltstone Member|30378|6|Mentioned|p432|||||||||
26403|Blowhole Creek Siltstone Member|30381|6|Mentioned|Table 1|||||||||
26403|Blowhole Creek Siltstone Member|39350|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26403|Blowhole Creek Siltstone Member|40454|6|Mentioned|Table 1|||||||||
26403|Blowhole Creek Siltstone Member|41947|5|Briefly described|p20|||||||||
26403|Blowhole Creek Siltstone Member|42270|4|Described|p361|||||||||
26403|Blowhole Creek Siltstone Member|42271|6|Mentioned|p378|||||||||
26403|Blowhole Creek Siltstone Member|43759|4|Described|p446|||||||||
26403|Blowhole Creek Siltstone Member|44133|5|Briefly described|p15|||Overlies: Madigan Inlet Member. ||||||
26403|Blowhole Creek Siltstone Member|50154|5|Briefly described|p52|||Of the Kanmantoo Group. Geological Province: Stansbury Basin.||||||
26403|Blowhole Creek Siltstone Member|60712|5|Briefly described|p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Carrickalinga Head Formation, Kanmantoo Group (Daily and Milne 1972, 1973).||||||31-MAY-05
26403|Blowhole Creek Siltstone Member|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of Carrickalinga Head Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||
27342|Blue Hills sandstone|30923|6|Mentioned|Map legend|Mesozoic|Paleozoic|Palaeozoic - Mesozoic||||||07-NOV-08
37129|Blue Mine Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
80326|Bluebush beds|70823|5|Briefly described|p44|Late Triassic|Late Triassic|Obsolete name of Price et al., 1985 that was replaced by the Cuddapan Formation.||||||31-JAN-18
26407|Blyth Dolomite Beds|29780|6|Mentioned|p21|||||||||
26407|Blyth Dolomite Beds|30801|6|Mentioned|p5|||River Wakefield Group. Table P5-6.||||||
26407|Blyth Dolomite Beds|30807|6|Mentioned|p103|||Suggested map symbol.||||||
26407|Blyth Dolomite Beds|34535|6|Mentioned|Fig.19|||||||||
26407|Blyth Dolomite Beds|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26407|Blyth Dolomite Beds|34587|5|Briefly described|p36|||||||||
26407|Blyth Dolomite Beds|35328|6|Mentioned|p11|||Now Blyth Dolomite||||||
26407|Blyth Dolomite Beds|44659|5|Briefly described|map legend|||Willouran, Lithology.||||||
26407|Blyth Dolomite Beds|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|Appears in Fig.9 without the lithology/rank.||Unit in River Wakefield Subgroup.||||
26407|Blyth Dolomite Beds|71237|14|Not recorded|p9, 17|||New name.||||||
80297|Blyth dolomite beds|71239|14|Not recorded|p5, p9, p17|||Shown as Blyth dolomite on p5.||||||
40456|Bob's Knob pegmatite|24593|6|Mentioned|p619|||Informal name for garnet pegmatite in the vicinity of The Needles west of Arkaroola Village.  See also p612 Fig. 1a and p620 Tb. 3.||||||
24740|Boconnoc Formation|22889|4|Described|p33 & p38|Adelaidean|Adelaidean|Boconnoc Formation superseded by Boconnoc Siltstone Member, as the unit has been down graded from formation to member status see p33 for details of change.||||||
24740|Boconnoc Formation|30801|6|Mentioned|p5|||River Wakefield Group. Table P5-6||||||
24740|Boconnoc Formation|30807|6|Mentioned|p103|||Suggested map symbol.||||||
24740|Boconnoc Formation|32725|6|Mentioned|p6|||Geological map.||||||
24740|Boconnoc Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24740|Boconnoc Formation|34587|5|Briefly described|p36|||||||||
24740|Boconnoc Formation|35328|6|Mentioned|Table 1|||||||||
24740|Boconnoc Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24740|Boconnoc Formation|40294|6|Mentioned|Table 2|||||||||
24740|Boconnoc Formation|41404|4|Described|p92|||||||||
24740|Boconnoc Formation|42222|6|Mentioned|Table 1 P4|||||||||
24740|Boconnoc Formation|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
24740|Boconnoc Formation|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|||Unit in River Wakefield Subgroup.||||
24740|Boconnoc Formation|71237|14|Not recorded|p9, 17|||||||||
25705|Bolla Bollana Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25705|Bolla Bollana Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yudnamutana Subgroup (Umberatana Group). Referred to as Bolla Bollana Tillite in main index!||||||
25705|Bolla Bollana Formation|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25705|Bolla Bollana Formation|23411|6|Mentioned|Map Legend|||||||||
25705|Bolla Bollana Formation|23818|4|Described|p64 Fig.22|Neoproterozoic|Neoproterozoic|Of the Yudnamutana Sub-Group. Underlying unit: Fitton Formation. Overlying unit: Lyndhurst Formation. Max. thickness: 7000 ft.||||||
25705|Bolla Bollana Formation|24176|4|Described|p11, p25 Tb. 1|Adelaidean|Adelaidean|Of Yudnamutana Sub-Group (Umberatana Group).  Boulder greywacke tillite.  Overlain by Lyndhurst Formation; underlain by and intertongued with Fitton Formation.  Age is Sturtian.  Max. thickness: 1860m.  Geological Province: Mount Painter Province.||||||
25705|Bolla Bollana Formation|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Glacial tillite. Of Umberatana Group. Overlies Fitton Formation. Overlain by Lyndhurst Formation. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25705|Bolla Bollana Formation|30176|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
25705|Bolla Bollana Formation|30177|4|Described|p72|||See also P73-75.||||||
25705|Bolla Bollana Formation|30376|6|Mentioned|p75|||See also P77||||||
25705|Bolla Bollana Formation|30621|6|Mentioned|p501|||Stratigraphy - Precambrian glaciation||||||
25705|Bolla Bollana Formation|30801|6|Mentioned|p5|||Yudnamutana Sub-Group. Table P5-6||||||
25705|Bolla Bollana Formation|30807|6|Mentioned|p103|||Suggested map symbol.||||||
25705|Bolla Bollana Formation|30810|6|Mentioned|p2|||Probable equivalent of Pualco Tillite||||||
25705|Bolla Bollana Formation|30920|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
25705|Bolla Bollana Formation|31797|6|Mentioned|Fig. 2|||Adelaidean. Yudnamutana Sub-Gp.||||||
25705|Bolla Bollana Formation|32364|1|Redefined|p15|Precambrian|Precambrian|Sturtian||||||
25705|Bolla Bollana Formation|32724|6|Mentioned|Fig.1|||Sturtian. Correlation||||||
25705|Bolla Bollana Formation|33474|6|Mentioned|Fig.2|||||||||
25705|Bolla Bollana Formation|34535|6|Mentioned|Fig.51|||||||||
25705|Bolla Bollana Formation|34536|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
25705|Bolla Bollana Formation|35255|6|Mentioned|p13|||||||||
25705|Bolla Bollana Formation|35628|6|Mentioned|Table 2|||||||||
25705|Bolla Bollana Formation|36137|6|Mentioned|p11|||||||||
25705|Bolla Bollana Formation|36253|6|Mentioned|Fig.3-2|||||||||
25705|Bolla Bollana Formation|37238|6|Mentioned|p353|||||||||
25705|Bolla Bollana Formation|37461|6|Mentioned|Fig.5.13|||||||||
25705|Bolla Bollana Formation|37932|6|Mentioned|p537|||||||||
25705|Bolla Bollana Formation|41364|6|Mentioned|p152|||||||||
25705|Bolla Bollana Formation|41405|4|Described|p132|||||||||
25705|Bolla Bollana Formation|41579|6|Mentioned|p14|||||||||
25705|Bolla Bollana Formation|41647|4|Described|p838|||||||||
25705|Bolla Bollana Formation|41770|6|Mentioned|p250|||||||||
25705|Bolla Bollana Formation|45149|6|Mentioned|Table 1|||Page 17.||||||
25705|Bolla Bollana Formation|60718|6|Mentioned|p52|||||||||
25705|Bolla Bollana Formation|67979|5|Briefly described|p529, p531 Fig.2|Sturtian|Sturtian|In Northern Flinders Ranges. Abruptly overlain by Tindelpina Shale Member in Yudnamutana area.||Yudnamutana Subgroup||abruptly overlain by Tindelpina Shale Member|dropstone shales and diamictites|
25705|Bolla Bollana Formation|69019|6|Mentioned|p43.|Neoproterozoic|Neoproterozoic|Of Coats (1964); subsequently Bolla Bollana Tillite (Coats and Forbes, 1977).||||||
25705|Bolla Bollana Formation|69023|5|Briefly described|p65|||Of Coats (1964); subsequently Bolla Bollana Tillite (Coats and Forbes, 1977).|||||A thick unit of massive boulder tillite consisting of abundant boulders set in a green or blue, gritty sub-greywacke matrix.|
25705|Bolla Bollana Formation|71237|2|Defined|p7, 8, 10, 17|||||||||
68697|Bolla Bollanna Formation|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Umberatana Group. Boulder tillite often with dark matrix.||||||11-JAN-10
79559|Bonney Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Pound Subgroup.||||
79559|Bonney Formation|73255|6|Mentioned|p542 Fig.10|Ediacaran|Ediacaran|[Misspelling of Bonney Sandstone?]||||||
28147|Bonney Sandstone Member|24176|4|Described|p15, p24 Tb. 1|Adelaidean|Adelaidean|Of Pound Quartzite - lower reddish hematitic and feldspathic sandstone and siltstone.  Age is Marinoan.  Intertongued with Rawnsley Quartzite Member.  Max. thickness: 400m.  Geological Province: Mount Painter Province.||||||
28147|Bonney Sandstone Member|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
28147|Bonney Sandstone Member|30220|6|Mentioned|Fig.13|||||||||
28147|Bonney Sandstone Member|30374|6|Mentioned|p27|||See also Fig.5. Unfossiliferous lower member of Pound Quartzite||||||
28147|Bonney Sandstone Member|30800|2|Defined|p219|Late Precambrian|Late Precambrian|||||||
28147|Bonney Sandstone Member|30802|5|Briefly described|p15|||Member of Pound Quartzite.||||||19-NOV-07
28147|Bonney Sandstone Member|31973|6|Mentioned|p3|||Correlation. Refers Forbes (1971)||||||
28147|Bonney Sandstone Member|35255|6|Mentioned|p32|||||||||
28147|Bonney Sandstone Member|37371|6|Mentioned|p384|||||||||
28147|Bonney Sandstone Member|37461|4|Described|p343|||||||||
28147|Bonney Sandstone Member|38970|6|Mentioned|p103|||||||||
28147|Bonney Sandstone Member|62453|4|Described|p12 Fig. 8|Ediacaran|Ediacaran|Geological Province: Adeliade Rift Complex/Stuart Shelf. Age: 556 +/- 24Ma. Of the Pound Subgroup.||||||
28147|Bonney Sandstone Member|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Ediacaran|Within Pound Subgroup. Dated at 556 +/- 24 Ma (Preiss, 2000).||||||19-MAR-12
28147|Bonney Sandstone Member|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Ediacaran|Within Pound Subgroup. Dated at 556 +/- 24 Ma (Preiss, 2000).||||||19-MAR-12
28147|Bonney Sandstone Member|69019|6|Mentioned|p61.|Neoproterozoic|Neoproterozoic|Mawson's (1938) informal subdivision of his Pound Quartzite into a lower red sandstone member and an upper white quartzite member was formalised by Forbes (1971) who defined them as Bonney Sandstone Member and Rawnsley Quartzite Member respectively. These were later (Jenkins, 1975) elevated to Formation status (within the Pound Subgroup).||||||
75013|Bonyeroo Formation|64455|6|Mentioned|p138 Fig. 1|Ediacaran|Ediacaran|Misspelling of Bunyeroo Formation.||||||29-JAN-09
67923|Book Limestone""|44133|6|Mentioned|p26|||Now part of the Moorowie Formation. Formerly included in the Billy Creek Formation. (Mount, 1970)||||||
76068|Bookpornong Formation|66286|6|Mentioned|p180 Fig.2.|||[Misspelling of Bookpurnong]||||||08-AUG-11
24751|Boorloo Siltstone""|37854|6|Mentioned|p12|||||||||
40218|Borda Formation, Lower|23792|5|Briefly described|Fig.D4|Hauterivian|Valanginian|Equivalent to Bronze Whaler supersequence. Overlies Neptune Formation. Overlain by Upper Borda Formation. Geological Province: Bight Basin.||||||
40218|Borda Formation, Lower|24201|5|Briefly described|p373 Fig. 2|Hauterivian|Valanginian|||||||
40218|Borda Formation, Lower|24338|5|Briefly described|p938 Fig. 2|Hauterivian|Valanginian|Overlain by the Upper Borda Formation. Overlies the Neptune Formation. Formation is Fm in text. Geological Province: Bight Basin||||||
40218|Borda Formation, Lower|24350|5|Briefly described|Fig. 4 Appdx|Hauterivian|Valanginian|Informal name. Part of Bronze Whaler Supersequence.||||||
40218|Borda Formation, Lower|24443|5|Briefly described|Fig.7|Hauterivian|Valanginian|Overlies Neptune Formaiton. Overlain by Upper Borda Formation. Geological Province: Bight Basin.||||||
40218|Borda Formation, Lower|24553|5|Briefly described|Figs. 7,8 and 10|Early Cretaceous|Early Cretaceous|Informal - see Borda Formation. Geological Province: Duntroon Sub-basin. Part of the Bronze Whaler Supersequence.||||||07-FEB-11
40218|Borda Formation, Lower|61630|6|Mentioned|p555 Fig. 3, p557|Early Cretaceous|Early Cretaceous|Informal name, refers to the lower part of the Borda Formation. Geological Province: Bright and Duntroon Basins.||||||
40218|Borda Formation, Lower|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Hauterivian|Valanginian|Ceduna and Duntroon Sub-basins. Deposited in fluvial channel, floodplain and lacustrine environments. Contains good potential seal facies. See also p39 fig 2.14, p58, p60, p64.  ||||Overlain by the Borda Formation, Upper. Overlies the Neptune Formation.|Mudstones.|
40218|Borda Formation, Lower|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Hauterivian|Valanginian|Bight Basin.||||Overlies Neptune Formation. Is overlain by Upper Borda Formation.||
40217|Borda Formation, Upper|23792|5|Briefly described|Fig.D4|Albian|Barremian|Equivalent to Bronze Whaler supersequence. Overlies Lower Borda Formation. Overlain by Ceduna Formation. Geological Province: Bight Basin.||||||
40217|Borda Formation, Upper|24201|5|Briefly described|p373 Fig. 2|Albian|Barremian|||||||
40217|Borda Formation, Upper|24338|5|Briefly described|p938 Fig. 2|Albian|Barremian|Overlain by the Ceduna Formation. Overlies the Lower Borda Formation. Formation is Fm in text. Geological Province: Bight Basin.||||||
40217|Borda Formation, Upper|24350|5|Briefly described|Fig. 4 Appdx|Albian|Barremian|Informal name. Part of Bronze Whaler Supersequence.||||||
40217|Borda Formation, Upper|24443|5|Briefly described|Fig.7|Albian|Barremian|Overlies Lower Borda Formation. Overlain by Ceduna Formation. Geological Province: Bight Basin.||||||
40217|Borda Formation, Upper|24553|5|Briefly described|p36, Figs. 7,8 and 10|Early Cretaceous|Early Cretaceous|Informal - see Borda Formation. Geological Province: Duntroon Sub-basin. Part of the Bronze Whaler Supersequence.||||||07-FEB-11
40217|Borda Formation, Upper|61630|6|Mentioned|p554, p555 Fig. 3, p556-559|Late Cretaceous|Early Cretaceous|Informal name used to refer to the upper part of the Borda Formation.||||||07-APR-09
40217|Borda Formation, Upper|69297|5|Briefly described|p14 fig 2.4, p25 fig 2.9|Albian|Hauterivian|Ceduna and Duntroon Sub-basins. Deposited in fluvial channel, floodplain and lacustrine environments. Contains good potential seal facies. See also p39 fig 2.14, p58, p60, p63, p64. ||||Overlies the Borda Formation, Lower. Overlain by the Ceduna Formation.|Fine-grained, well-sorted feldspathic litharenites and mudstones.|
40217|Borda Formation, Upper|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Albian|Barremian|Bight Basin.||||Overlies Lower Borda Formation. Is overlain by Ceduna Formation.||
70784|Bosanquet Volcanics|67536|5|Briefly described|Map Legend|Orosirian|Orosirian|Gawler Craton.|1859 +/- 11 Ma||||Rhyodacite and calcsilicate rock.|
38345|Bosanquet formation|23791|6|Mentioned|p4|||||||||
38345|Bosanquet formation|61307|5|Briefly described|p37|||Informal name. Of the Hutchison Group (upper part). Interlayered diopside-rich calc-silicates and felsic gneisses. Geological Province: Gawler Craton. ||||||
81680|Boucaut volcanics|63102|5|Briefly described|p46,49,53,63|Tonian|Tonian|Of Adelaide Geosyncline. Felsic volcanis, represents early stages of extensional rifting of Adelaide Geosyncline. Extruded at or below the base of Burra Group.|~777 Ma|||||
82099|Box Bore granite|72459|5|Briefly described|p59, p65-66, p69, p73, p94, p100|Mesoproterozoic|Mesoproterozoic|Forms subgroup 2c of the Moolawatana Suite in this report which includes: the Box Bore granite, a pod of microgranite north of Pepagoona Well adjacent to the Pepagoona Porphyry and a number of microgranites and porphyries previously analysed by Sheard during mapping of the MOOLAWATANA 1:50k sheet. Strongly deformed and fabric is in places mylonitic.|c. 1555 Ma (U-Pb zircon, Sheard, 1997)|Moolawatana Suite|||Coarse-grained, pink to white, megacrystic granite/augen gneiss.|
39974|Brachina Formation, Lower|24195|6|Mentioned|p42|||Not intended as a formal name - see Brachina Formation. Overlain by Port Stanvac Sandstone Member.||||||20-FEB-08
39972|Brachina Formation, Upper|24195|6|Mentioned|p42,48|||Not intended as a formal name - see Brachina Formation||||||
74125|Brachina Group|62962|6|Mentioned|p2296 Tab. 6|||Geological Province: Mount Painter Province.||||||07-FEB-11
74125|Brachina Group|71139|6|Mentioned|p153||||547-544 Ma (deformation).|||||
25707|Brachina Subgroup|34901|6|Mentioned|p15|||||||||
25707|Brachina Subgroup|35317|6|Mentioned|p395|||||||||
25707|Brachina Subgroup|35586|1|Redefined|p26|late Adelaidean|late Adelaidean|||||||
25707|Brachina Subgroup|36011|6|Mentioned|p13|||||||||
25707|Brachina Subgroup|37015|5|Briefly described|p68|||See also Fig.2.||||||
25707|Brachina Subgroup|37627|6|Mentioned|p188|||||||||
25707|Brachina Subgroup|37716|6|Mentioned|p1152|||||||||
25707|Brachina Subgroup|40456|6|Mentioned|p19|||||||||
25707|Brachina Subgroup|40852|6|Mentioned|Fig.3.7|||||||||
25707|Brachina Subgroup|41236|4|Described|p63|||||||||
25707|Brachina Subgroup|42240|6|Mentioned|p173|||||||||
25707|Brachina Subgroup|42243|5|Briefly described|p209|||||||||
25707|Brachina Subgroup|42813|6|Mentioned|p22|||||||||
81372|Braemar iron formation|70323|6|Mentioned|p212,219|||Southern Flinders Ranges, Adelaide geosyncline. ||||Correlable to Holowilena Ironstone.||
75794|Breaden Hill  Megabreccia|60718|5|Briefly described|p51, 53, 54|Adelaidean|Adelaidean|Supersedes Breaden Megabreccia. Interpreted as an allochthonous salt canopy, extruded post-Skillogalee Dolomite and subsequently deflated. Contains large xenoclasts of Black Knob Marble, Noranda Volcanics, Dome Sandstone within yellow flow-banded dolomite matrix.||||Overlies Boorloo Siltstone.||15-APR-11
39668|Breaden Megabreccia""|24175|5|Briefly described|p9|||Nomenclature attributed to Murrell (1977).||||||
39581|Bremer Greywacke|24465|5|Briefly described|p346 Fig.3|||Of Mirams, 1962 - of the Brukunga Formation.  Probably superseded.||||||19-JAN-05
67943|Bridgewater Formation calcarenites|44133|6|Mentioned|p259|||Informal, refers to Bridgewater Formation. ||||||
42495|Bridgewater Formation, Lower|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Otway Basin.||||||
42495|Bridgewater Formation, Lower|62893|4|Described|Map Legend, p23-24|Pleistocene|Pleistocene|Interbedded with Ripon Calcrete. Commonly capped by a dense, very hard, pinkish calcrete.||||Equivalent to Ripon Calcrete.|White to fawn aeolian calcarenite with very large foresets (up to 10 m) and interlayered reddish brown clay, silt and loess with dispersed calcrete clasts.|
42496|Bridgewater Formation, Upper|23818|5|Briefly described|p212 Fig.108|Middle Pleistocene|Middle Pleistocene|Geological Province: Otway Basin.||||||
42496|Bridgewater Formation, Upper|62893|4|Described|Map Legend, p23|Pleistocene|Pleistocene|Interbedded with Bakara Calcrete. Also intertongues with a white fossiliferous lacustrine limestone (Qpl) containing abundant moulds of Coxiella striata (Ludbrook, 1984). Jaw bone of a Diprotodontid was recovered from this unit.||||Equivalent to Bakara Calcrete.|Soft white, cream and fawn aeolian calcarenite with very large foresets, white silt and loess.|
81625|Brighton Limestone Member|72247|6|Mentioned|p41|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||||
28400|Brighton Limestone""|32724|6|Mentioned|Fig.1|||Correlation. Sturtian||||||
80469|Brindina Schist|67323|5|Briefly described|p36|||Mount Painter Inlier, northern Gawler Craton.|~1600-1590 Ma protolith deposition.|||||
80469|Brindina Schist|71531|14|Not recorded|p9, 11|||||||||
23420|Bring Member|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Eocene|||||||
23420|Bring Member|22613|4|Described|p19|||Pidinga Formation||||||
23420|Bring Member|23331|6|Mentioned|1089|||||||||
23420|Bring Member|23488|5|Briefly described|p40|Late Eocene|Late Eocene|Spicular.  Of the Pidinga Formation.  Geological Province: Eucla Basin.||||||
23420|Bring Member|23533|5|Briefly described|p564 Fig 3|Late Eocene|Middle Eocene|Geological Province: Eucla Basin.||||||
23420|Bring Member|24396|5|Briefly described|p222 Fig.5|Late Eocene|Late Eocene|Of Pidinga Formation in previous nomenclature. Unclear what it equates to in this study: either upper Pidinga Fm or Khasta Fm.||||||22-JAN-15
23420|Bring Member|24397|5|Briefly described|p242|||Formerly of the Pidinga Formation.  Now included in the Khasta Formation.  Geological Province: Eucla Basin.||||||22-JAN-15
23420|Bring Member|24617|6|Mentioned|p115 Fig. 3|Eocene|Eocene|Nomenclature from previous work of Benbow 1993; Benbow et al. 1995 and Alley et al. 1999. Name may now be superseded. Geological Province: Eucla Basin.||||||
23420|Bring Member|40912|6|Mentioned|Map legend|late Eocene|late Eocene|Latest Eocene||||||
23420|Bring Member|42475|5|Briefly described|p20|||of Pidinga Formation||||||
23420|Bring Member|42816|5|Briefly described|p22|||of Pidinga Formation||||||
23420|Bring Member|44133|5|Briefly described|p180|Late Eocene|Late Eocene|Geological Province: Eucla Basin. Of the Pidinga Formation.||||||
23420|Bring Member|44695|5|Briefly described|Map Legend|Eocene|Eocene|(Middle-Late Eocene)||||||
23420|Bring Member|61155|5|Briefly described|p17|Late Eocene|Late Eocene|Of the Pidinga Formation. Geological Province: Eucla Basin.||||||
23420|Bring Member|61856|5|Briefly described|p313|||With the former Khasta Member, now Khasta Formation.||Unit of Pidinga Formation.||||
40457|British Empire Granite""|24593|6|Mentioned|p619|||Informal - see British Empire Granite.  Applied to S-type granite phase only.||||||
37476|British Empire Type Granite|24045|6|Mentioned|p533 Fig.2||Ordovician|Informal name.||||||
73829|British Empire granite|24546|5|Briefly described|p2 - 14 Fig.7|Paleozoic|Paleozoic|Informal. Possible intrusion at about 400 Ma. Intrudes Mount Painter Province.||||||07-NOV-08
68101|Broken Hill Group, lower|60485|6|Mentioned|p26|||Informal - see Broken Hill Group.||||||
69470|Broken Hill gabbro|61154|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Informal name. Age: ~820Ma. Part of extensive mafic magmatism together with the Gairdner Dyke Swarm. Geological Province: South Australian Craton.||||||
39209|Broughton River Slate|23731|5|Briefly described|p27|||Of Tapley Hill Formation.||||||
39209|Broughton River Slate|64769|6|Mentioned|p27|||Dimension stone name.||||||06-MAY-09
24771|Brown Hill Sub-group|30380|6|Mentioned|Table 1|||Correlation||||||
24771|Brown Hill Sub-group|30381|4|Described|p216|||||||||
24771|Brown Hill Sub-group|40442|6|Mentioned|p17|||||||||
28403|Brownhill Greywacke Member|23818|4|Described|p101 Fig.43, p106|Cambrian|Cambrian|Geological Province: Kanmantoo Trough. Uppermost unit of the Brukunga Formation. Max. thickness: 12 000 ft.||||||
28403|Brownhill Greywacke Member|32321|6|Mentioned|Table 2|||||||||
28403|Brownhill Greywacke Member|33471|5|Briefly described|p557|||||||||
28403|Brownhill Greywacke Member|34612|5|Briefly described|p106|||Kanmantoo Group||||||
28403|Brownhill Greywacke Member|36836|6|Mentioned|p39|||||||||
24772|Browns Creek Clays|24551|6|Mentioned|p297 Fig. 10.7|||Informal: see Browns Creek Clay.||||||
24772|Browns Creek Clays|39923|6|Mentioned|p354|||||||||
24772|Browns Creek Clays|43748|6|Mentioned|App 1|||Otway Basin. Used in palaeomagnetic pole comparision.||||||
24772|Browns Creek Clays|62896|5|Briefly described|p87|Eocene|Eocene|Geological Province: Otway Basin.||||||07-FEB-11
24772|Browns Creek Clays|62899|6|Mentioned|p46|Late Eocene|Late Eocene|Contains ostracods.||||||
24772|Browns Creek Clays|63740|5|Briefly described|p87, p102|Late Eocene|Eocene|Geological province: Otway Basin. Ostracod fragment at Castle Cove.||||||07-FEB-11
26427|Brukunga Formation|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Kanmantoo Group. Interbedded phyllites and greywacke with lenticular pyritic and calc-silicate lenses. Includes the Brown Hill Greywacke Member and the Nairne Pyrite Member.||||||
26427|Brukunga Formation|23818|4|Described|p100 Fig.42|Early Cambrian|Early Cambrian|Geological Province: Kanmantoo Trough. Uppermost unit of the Kanmantoo Group. Max. thickness: ~24 000 ft.||||||18-APR-05
26427|Brukunga Formation|24465|5|Briefly described|p346 Fig.3|||Probably superseded. Shown as out of use since 1962.||||||11-OCT-12
26427|Brukunga Formation|29406|6|Mentioned|p53|||||||||
26427|Brukunga Formation|29697|5|Briefly described|Table 3|||||||||
26427|Brukunga Formation|30051|6|Mentioned|Fig.1|||||||||
26427|Brukunga Formation|30377|6|Mentioned|Table 2|||||||||
26427|Brukunga Formation|30380|6|Mentioned|Table 1|||Refers Thomson in Parkin(1969)||||||
26427|Brukunga Formation|30381|6|Mentioned|p215|||Term discarded||||||
26427|Brukunga Formation|30754|6|Mentioned|p10|||Map||||||
26427|Brukunga Formation|30755|6|Mentioned|p168|||Tectonic Map||||||
26427|Brukunga Formation|30801|6|Mentioned|p5|||Kanmantoo Group. Table P5-6||||||
26427|Brukunga Formation|30807|6|Mentioned|p102|||Suggested map symbol.||||||
26427|Brukunga Formation|31554|6|Mentioned|p13|||||||||
26427|Brukunga Formation|31923|6|Mentioned|p11|||||||||
26427|Brukunga Formation|32321|6|Mentioned|p82|||||||||
26427|Brukunga Formation|32432|6|Mentioned|Fig.2|||See also Table 1||||||
26427|Brukunga Formation|33471|5|Briefly described|p557|||||||||
26427|Brukunga Formation|33634|6|Mentioned|p562|||||||||
26427|Brukunga Formation|34195|6|Mentioned|p1|||See also PP2,3.||||||
26427|Brukunga Formation|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
26427|Brukunga Formation|34612|6|Mentioned|Fig.43|||||||||
26427|Brukunga Formation|34617|6|Mentioned|p2|||||||||
26427|Brukunga Formation|35027|6|Mentioned|p385|||||||||
26427|Brukunga Formation|35358|6|Mentioned|p18|||Relationship to Rathjen Gneiss.||||||
26427|Brukunga Formation|36836|4|Described|p42|||||||||
26427|Brukunga Formation|39132|6|Mentioned|p189|||||||||
26427|Brukunga Formation|40856|6|Mentioned|Fig.23.6|||||||||
26427|Brukunga Formation|60712|5|Briefly described|p30 Fig. 3|Early Cambrian|Early Cambrian|Replaced Brown Hill Beds (Forbes (1957).  Included all Kanmantoo Gp metsediments above Inman Hill Fm. Superseded by Brownhill and Wattaberri Subgroups. Contains several carbonaceous phyllitic members at different levels.||||||31-MAY-05
26427|Brukunga Formation|61556|5|Briefly described|p9-10 Figure||Cambrian|In Mount Lofty ranges, Adelaide Syncline.||||||
68723|Bryant Creek formation, upper|24558|6|Mentioned|p664, p666|Miocene|Miocene|Informal - see Bryant Creek Formation.||||||
41590|Buccleuch Group""|23671|5|Briefly described|p3|Eocene|Eocene|Informal name.  Probably interdigitates with the Renmark Beds.||||||16-AUG-04
76833|Buckelboo Granite|67028|6|Mentioned|p373|||Mis-spelling of Buckleboo Granite.||||||24-APR-12
41671|Buckleboo granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Of the Kokatha suite. Age: 1592Ma.||||||07-FEB-11
41671|Buckleboo granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
78304|Bulldog Shale Formation|68821|6|Mentioned|p301 Fig.5|||Misspelt Bulldog Shale in figure||||||
76760|Bumba Formation|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Olary Block, South Australian Craton. Calcsilicate part shown in Fig.5.||Of Willyama Supergroup.||||11-APR-12
67944|Bumbunga Sand Member|44133|5|Briefly described|p164, 152 Fig. 10.2|Oligocene|Eocene|Of the Clinton Formation. Geological Province: Saint Vincent Basin. Thickness: 30m.||||||
75963|Buneyeroo Formation|63811|6|Mentioned|p503|Ediacaran|Ediacaran|Of Wilpena Group, Stuart Shelf. [Mis-spelling of Bunyeroo]||||||28-MAR-12
34760|Bungarider Subgroup""|22889|5|Briefly described|p31 & p35|Adelaidean|Adelaidean|This name lapsed from reservation so it is proposed here to resurrect the term Bungarider Subgroup with a new Definition, see p 35 for details on change.||||||
37124|Bunyeroo formation|23562|6|Mentioned|p294|||Informal.||||||
81233|Bunyeroo red beds|68030|4|Described|p238|Ediacaran|Ediacaran|Flinders Ranges.  Informally (?) named by Schmidt and Williams, 1996. occurs about 80m above the base of the Bunyeroo Formation. This layer is a regional chronostratigraphic marker; interpreted to be debris from a bolide impact (Gostin et al., 1986), with comparable lithology and U-Pb geochronology to the Gawler Rangew Volcanics. Impact structure is likely to be Acraman impact structure (accordant paleomagnetic data for Acraman belt rock and Bunyeroo red beds; Schmidt and Williams, 1996). ||Unit of Bunyeroo Formation? or equivalent?||Surrounded by Bunyeroo Formation sediments.|A single layer of angular fragments of red, porphyritic dacite is embedded in shale (10-20cm above and below altered to green colour) and overlain by a 1-10 cm of graded sand and granules with swaley cross-lamination.|07-AUG-19
40388|Bunyeroo shale|24484|5|Briefly described|p804|||Overlain by the Wonoka Formation. Informal name.||||||
34074|Burdunga Beds|22613|6|Mentioned|p17|Neoproterozoic|Neoproterozoic|Officer Basin||||||
28417|Burr Complex|32417|6|Mentioned|p2|||||||||
24796|Burra Group megabreccias|35904|6|Mentioned|p9|||||||||
39672|Burra Group siltstone|24175|6|Mentioned|p15|Paleozoic|Paleozoic|Informal name - see Burra Group.||||||07-NOV-08
72805|Burra Group, Lower|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Informal - see Burra Group.  Together with Middle Burra Group consists of mainly siltstone and dolomite. Max. thickness: ~2km.||||||07-FEB-07
72806|Burra Group, Middle|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Informal - see Burra Group.  Together with Lower Burra Group consists of mainly siltstone and dolomite.||||||07-FEB-07
72807|Burra Group, Upper|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Informal - see Burra Group.  Represents a transgressive cycle, comprising mainly silty and carbonaceous dolomite, quartzite, shale and siltstone.||||||07-FEB-07
72807|Burra Group, Upper|42222|4|Described|p14|||||||||
72807|Burra Group, Upper|42236|6|Mentioned|Fig.2 P106|||||||||
39677|Burra Group, lower|22510|6|Mentioned|p37 Table 1|Adelaidean|Adelaidean|Informal - see Burra Group.||||||13-OCT-04
39677|Burra Group, lower|24175|6|Mentioned|p10|||Informal - see Burra Group.||||||
41872|Burra Group, middle|22510|6|Mentioned|p37 Table 1|Adelaidean|Adelaidean|Informal - see Burra Group.||||||
39896|Burra Group, upper|24175|6|Mentioned|p12|||Informal name - see Burra Group||||||
39896|Burra Group, upper|63250|6|Mentioned|p6|||Informal name. Absent in Tasmania. Stated to be 2-3km thick where it occurs. ||||||
81623|Burra porphyry|72238|5|Briefly described|p42|Tonian|Tonian|Of Adelaide Geosycline. Age quoted as 794+\-4 Ma, but no reference (p42).|794+\-4 Ma|||||
28009|Bute Amphibolite|22629|5|Briefly described|p153|Proterozoic|Proterozoic|Now Bute Metasediments||||||07-MAR-16
28009|Bute Amphibolite|23719|6|Mentioned|p18|||Of Thomson, 1973.||||||24-JUN-09
28009|Bute Amphibolite|24475|6|Mentioned|p48, p56|||Redefined as Bute Metadolerite.||||||
28009|Bute Amphibolite|43052|5|Briefly described|p68|||||||||
28228|Byilkaoora Formation|22746|5|Briefly described|Fig.3 p515|Late Cambrian|Late Cambrian|||||||
28228|Byilkaoora Formation|23288|6|Mentioned|Fig.5||Early Ordovician|||||||
28228|Byilkaoora Formation|23524|5|Briefly described|p221 Fig. 3|Ordovician|Ordovician|||||||
28228|Byilkaoora Formation|23858|5|Briefly described|p917|Ordovician|Cambrian|Geological Province: Officer Basin.||||||
28228|Byilkaoora Formation|38329|2|Defined|p207|Early Ordovician|Early Ordovician|Prob.Early Ordovician||||||
28228|Byilkaoora Formation|40945|6|Mentioned|Fig.3|||||||||
28228|Byilkaoora Formation|43657|6|Mentioned|Fig.3,p4||Ordovician|||||||
28228|Byilkaoora Formation|43732|6|Mentioned|Fig.4,p5||Late Cambrian|||||||
28228|Byilkaoora Formation|44109|5|Briefly described|p22 Fig. 21|Ordovician|Ordovician|Geological Province: central Officer Basin.||||||
28228|Byilkaoora Formation|44133|4|Described|p40, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Overlies: Trainor Hill Sandstone. Disconformably overlies: Mount Johns Conglomerate. Underlies conformably the Mount Chandler Sandstone. Maximum Thickness: ~15m.||||||07-NOV-08
39195|Cadell Marl member|23768|5|Briefly described|p108|||Informal - see Cadell Marl. Of Morgan Limestone.||||||
39187|Cadell formation|23768|6|Mentioned|p34|||Informal - see Cadell Formation, Cadell Marl.||||||29-MAR-05
31399|Cadna Owie Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|Probably misspelling of Cadna-owie Formation||||||
31399|Cadna Owie Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Late Jurassic|Probably should be Cadna-owie Formation? See also Cadnaowie Formation. Thickness: 900m. Geological province: Eromanga Basin. Marginal marine to non-marine deposits.||||||
23453|Cadnawitana Formation""|38926|6|Mentioned|p37|||||||||
34534|Cadney Park Formation|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|||||||
34534|Cadney Park Formation|23524|5|Briefly described|p221 Fig. 3|Early Cambrian|Early Cambrian|||||||
34534|Cadney Park Formation|24112|5|Briefly described|p54 Fig.2, p257 Tb.1|||Age: 524-522Ma. Geological Province: Officer Basin||||||
33991|Calc-silicate Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
33991|Calc-silicate Suite|23869|5|Briefly described|p13|||Not a formal name.||||||
33991|Calc-silicate Suite|24307|5|Briefly described|p968 Fig. 3|||Informal terminology used by Clarke, 1986 and Ashley et al, 1966, for the Olary Domain.||||||
33991|Calc-silicate Suite|24592|5|Briefly described|p635|||Overlain by the Pelite Suite. Overlies the Quartzo-feldspathic Suite. Of the Willyama Supergroup. Geological Province: Curnamona Province. Interbedded calc-silcate & albitic siltstone. A magnetic susceptibility division of the Willyama Supergroup.||||||
42319|Calca Red Granite|60566|6|Mentioned|p28|||Also marketed as Empire Red granite.||||||07-DEC-04
39207|Calca Red granite|23731|6|Mentioned|p26|||Informal name for deimension stone of Hiltaba Suite granite.||||||
39207|Calca Red granite|60496|5|Briefly described|p23|||Commercial name for Claca Granite monumental stone.  Granular mosaic of equant anhedral crystals of quartz and feldspar set in a fine-grained matrix of quartz and feldspar with traces of biotite, chlorite and hornblende.  red colour due to fine inclusions||||||
30092|Calcsilicate Suite|23248|5|Briefly described|Fig2p169|||||||||
30092|Calcsilicate Suite|43086|5|Briefly described|p3|||Not to be viewed as a strict stratigraphic unit.||||||
30092|Calcsilicate Suite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Olary Domain. Informal name.||Unit in Willyama Supergroup.||Overlies Quartzo-feldspathic Suite. Is overlain by Bimba Suite.||
75080|Calcsilicate Suite""|64944|6|Mentioned|p27|Paleoproterozoic|Paleoproterozoic|Informal name of Clarke et al (1986) generally equivalent to the Ethiudna Subgroup (lower Curnamona Group).||||||07-FEB-11
27358|Callabonna Soil|38604|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27358|Callabonna Soil|38605|6|Mentioned|p41|||||||||
27358|Callabonna Soil|42720|5|Briefly described|map legend|Pleistocene||||||||
27358|Callabonna Soil|42813|6|Mentioned|p25|||||||||
34586|Callamurra Sandstone Member|22839|6|Mentioned|p33|||||||||10-DEC-15
73830|Callana beds|24546|6|Mentioned|p2 - 4 Fig.3|||Geological Province: Adelaide Fold Belt.||||||09-JAN-08
73830|Callana beds|61556|5|Briefly described|p9-10 Figure|Adelaidean|Adelaidean|Written as Callana Beds - p11.||||||21-NOV-07
70775|Callana group|61308|6|Mentioned|p6|||Informal - see Callana Group.||||||
42498|Callanna Beds, Lower|23818|6|Mentioned|p36 Fig.9|Adelaidean|Adelaidean|||||||
42499|Callanna Beds, Upper|23818|6|Mentioned|p36 Fig.9|Adelaidean|Adelaidean|Max. thickness: 7000 ft.||||||
39676|Callanna Group, upper|22857|6|Mentioned|p65|||Informal - see Callana Group. Shallow marine sediments.||||||
39676|Callanna Group, upper|24175|6|Mentioned|p10|||Informal - see Callanna Group.||||||
39676|Callanna Group, upper|60718|6|Mentioned|p49, p50|||Informal - see Callanna Group. Evaporitic sediments. See also p53 Fig. 4.||||||15-APR-11
24808|Callanna beds""|37854|6|Mentioned|p7|||||||||
24808|Callanna beds""|40294|6|Mentioned|p8|||||||||
24808|Callanna beds""|41403|6|Mentioned|p43|||||||||
23462|Camel Flat Shale""|38926|5|Briefly described|p34|||||||||
23462|Camel Flat Shale""|42238|6|Mentioned|p73|||||||||
69042|Campana Creek Sandstone Member|60712|5|Briefly described|p30 Fig. 3, p37|Early Cambrian|Early Cambrian|Of Daily and Milnes (1972, 1973).  Of the Carrickalinga Head Formation (Kanmantoo Group).||||||31-MAY-05
73610|Cannela beds|63489|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Very deformed phyllite. minor sandstone, silicic tuff.||||||10-SEP-07
73610|Cannela beds|66623|6|Mentioned|p88.|||Term used by Mills (2003) for rocks previously part of Wonominta beds (Warris 1967). Redefined as Cannela Formation in this study.||||||
73610|Cannela beds|66933|5|Briefly described|Map legend|Cambrian|Cambrian|Milparinka Zone, Delamerian Fold Belt.|||||Phyllite, cleaved metasandstone, turbiditic metasandstone and abundant very fine rhyolitic tuffs of cherty appearance.|
41672|Cape Colbert granite|50605|5|Briefly described|p5.2|Paleoproterozoic|Paleoproterozoic|Of the Younger Lincoln Supersuite. Geological Province: Gawler Craton & Curnamona Province.||||||07-NOV-08
41673|Cape Colbert hornblende granite|24197|6|Mentioned|p74 Tb. 8.1|||Informal name. Geological Province: Gawler and Curnamona Cratons.||||||07-FEB-11
41673|Cape Colbert hornblende granite|50605|5|Briefly described|p1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Younger Lincoln Supersuite. Age: 1757 +/- 14Ma (Rb-Sr).||||||07-NOV-08
40383|Cape Jervis Formation, Lower|24360|6|Mentioned|p55 Fig. 2|||Informal - see the Cape Jervis Formation||||||
40384|Cape Jervis Formation, Upper|24360|6|Mentioned|p55 Fig. 2|||Informal - see the Cape Jervis Formation.||||||
26457|Cape Jervis beds|39929|6|Mentioned|p276|||||||||
26457|Cape Jervis beds|40324|6|Mentioned|p62|||||||||
26457|Cape Jervis beds|41495|4|Described|p42|||||||||
26457|Cape Jervis beds|41684|6|Mentioned|p2|||||||||
26457|Cape Jervis beds|42093|5|Briefly described|p10|||See also Fig.5||||||
26457|Cape Jervis beds|42491|6|Mentioned|p7|||Troubridge Basin.||||||
26457|Cape Jervis beds|42506|5|Briefly described|Map legend|Permian|Carboniferous|||||||
26457|Cape Jervis beds|42733|5|Briefly described|map legend|Permian||||||||
26457|Cape Jervis beds|42966|6|Mentioned|p63|||||||||
26457|Cape Jervis beds|49040|6|Mentioned|p7|||||||||
26457|Cape Jervis beds|61314|6|Mentioned|p128|||Of South Australia, and correlate with unnamed sediments which are isolated remnants of Late Carboniferous to early Permian glaciomarine deposits preserved in infrabasins beneath the Murray Bain. ||||||
26457|Cape Jervis beds|65375|6|Mentioned|p32.|||Named by Ludbrook (1967); subsequently Cape Jervis Formation (Bourman and Alley 1990).||||||
26457|Cape Jervis beds|66623|6|Mentioned|p231.|Permian|Permian|Name superseded by Cape Jervis Formation.||||||
37078|Capra Granite|23719|4|Described|p19|Calymmian|Statherian|Age: 1677+/-125 Ma (Rb-Sr). See also page 15 table 2, page 19 table 5. Part of Lincoln Complex. Geological Province: Gawler Craton.||||||05-MAR-08
42318|Carey Gully Sandstone|60566|5|Briefly described|p28-29|||Fine grained sandstone. Used as a building stone in Adelaide.||||||
34658|Carey Gully Sandstone""|22869|6|Mentioned|P38|||Superseded by Carey Gully Sandstone Member||||||
24824|Carickalinga Head Formation|42788|5|Briefly described|Fig.14 P148|||of Kanmantoo Group||||||
39968|Carnarvon Greywacke Member|24195|5|Briefly described|p48|||Parent: Tapley Hill Formation. Geological Province: Adelaide Geosyncline||||||
39967|Carnarvon Greywacke Member, Upper|24195|6|Mentioned|p48|||Not intended as a formal name - see Carnarvon Greywacke Member||||||
78808|Carnding Rhyolite|64137|6|Mentioned|p1553 Fig.8|||Neodymium isotope data from Stewart (1994) thesis. Shown as Ealbara/Carnding Rhy. in figure and only expanded [wrongly] in figure caption.||||||17-MAR-14
35704|Cartu beds""|23282|6|Mentioned|p83|||Synonym of Blue Hills Sandstone.||||||
73539|Casterton beds""|63124|6|Mentioned|p55|||Of Wopfner et al 1971). Informal name - superseded by Casterton Formation. ||||||
80362|Cathedral Rock Metasandstone Member|63102|4|Described|p17,19|||Geological province: Olary Domain, Curnamona Province. Nomenclature of Zang (pers. comm., 2002). Relatively persistent quartzite-bearing horizon, which forms the base of the overlying Ethiudna Subgroup. Hosts mineralisation at the Mount Mulga Ba-Cu-Au Mine.|||||Quartzite; variably clean and cross-bedded to recrystallised to ferruginous and volcaniclastic to auriferous, baritic, iron formation.|
80362|Cathedral Rock Metasandstone Member|70657|5|Briefly described|p29|||A quartzite marker recognised by Campana and King (1958), Forbes (1991) and Conor (2000). The name Cathedral Rock Metasandstone Member was suggested by Zang (PIRSA, pers. comm., 2002); modified in this study to Cathedral Rock Formation||||||
40385|Cathedral Rock breccia|24431|5|Briefly described|p189 Fig. 1|||Geological Province: Olary Domain||||||
34571|Cattle Grid Breccia|22829|6|Mentioned|P16|||||||||
34571|Cattle Grid Breccia|70082|6|Mentioned|p2-10,16|Cryogenian|Cryogenian|Stuart Shelf. Reference section: (possibly? Not explicitly mentioned on p2) Mt Gunson Mine (S31.44278, E137.135350). Contains red beds and periglacial paleosols, correlable to Elatina Formation.||||||
34571|Cattle Grid Breccia|73227|5|Briefly described|p25, p27-29|||Mount Gunson area. Formed through in situ frost shattering of silicified Pandurra Formation during the Elatina (Marinoan) glaciation in the Adelaide Rift Complex. Includes periglacial structures.||||||
81669|Cattle Grid Formation|70334|5|Briefly described|p38,52|||Geological province: Gawler Craton. Of Stuart Shelf. Informal term used by exploration companies on the Stuart Shelf; equivalent to Whyalla Sandstone/Yerelina Subgroup, specifically stratigraphy between Brighton Limestone and Tent Hill Formation (Mason 1979).||||||
81626|Cattle Grid Formation''|71129|6|Mentioned|p111|||Of Stuart Shelf. Informal terminology referring to the combined 'Yudnapinna Beds'-Wilmington Formation and the overlying Whyalla Sandstone, used in the past by company geologists (Australian Selection Pty Ltd, 1979).||||||
81626|Cattle Grid Formation''|72247|6|Mentioned|p41, 44|Neoproterozoic|Neoproterozoic|Of Mason (1978).Of Stuart Shelf.||||||16-SEP-19
81700|Cattlegrid Sandstone Member''|71129|6|Mentioned|p110|||Of Stuart Shelf. Nomeclature of Australian Selection Pty Ltd, 1977b to describe sandstones and siltstones of the Upalinna and Yerelina subgroups.||||||13-NOV-19
80141|Chace Member|70790|5|Briefly described|p258 Fig.1, p259-260, p266-268, p270-271|Ediacaran|Ediacaran|Adelaide Rift Complex. Facies and depositional environment detailed.||Rawnsley Quartzite.||Unconformably overlies Bonney Sandstone.||
30340|Chace Quartzite|64829|6|Mentioned|p1101 Fig. 16A|||Shown in  Cambrian soilscape figure - underlies Ediacara Member of the Rawnsley Quartzite.||||||07-FEB-11
77400|Chamber Bluff Tillite|65376|6|Mentioned|p247 Fig.6.57.|Neoproterozoic|Neoproterozoic|||||||
77401|Charlestoin Granite|65376|6|Mentioned|p152.|||A mis-print of Charleston Granite.||||||
74962|Chase Quartzite Member|64455|5|Briefly described|p138 Fig. 1|Early Cambrian|Early Cambrian|Of Rawnsley Quartzite. Overlian by Ediacara Member.||||||29-JAN-09
74962|Chase Quartzite Member|64460|5|Briefly described|p197, p198|||Of Rawnsley Quartzite. Underlain by Bonney Sandstone. Thickness: 90m. White sandstones or quartzites.||||||
32775|Cheltenhamian Stage|44223|14|Not recorded|p.159|||||||||
32775|Cheltenhamian Stage|44238|14|Not recorded|p.227|||||||||
28450|Cherry Gardens black clay|32424|6|Mentioned|p11|||Sample collection||||||
78974|Childara Dacite|69649|4|Described|p17-19|Mesoproterozoic|Mesoproterozoic|[Repeated mis-spelling of Childera]. Giles (1977). Over 200m thick. Flint (1993) reported age of lower sequences (including Glyde Hill Volcanics Complex) from Fanning et al. (1988) as 1592+/-3 Ma.||Basal unit in Glyde Hill Volcanic Complex.||Is overlain conformably by Mangaroongah Dacite.|Dark grey basaltic andesite at base, grading into massive, aphyric purplish-red to red-brown dacite flows separated locally by epiclastic layers.|23-FEB-15
32470|Chinaman's Gully Beds|23818|6|Mentioned|p192|||Separates the Blanche Point Marls from the overlying Wilunga Beds.||||||
32470|Chinaman's Gully Beds|23828|5|Briefly described|p94|Late Eocene|Late Eocene|Geological Province: St Vincent Basin.  Maximum thickness: 2m.||||||
32470|Chinaman's Gully Beds|33330|14|Not recorded|Not recorded|||||||||
27742|Chinamans Gully Beds|30250|6|Mentioned|Table 2|||Misspelling of Chinaman Gully? Refers Reynolds(1953)||||||
27742|Chinamans Gully Beds|30251|6|Mentioned|p3|||Table on P3||||||
27742|Chinamans Gully Beds|31846|4|Described|Fig. 1|||See also P7||||||
27742|Chinamans Gully Beds|32117|6|Mentioned|Fig.2|||||||||
27742|Chinamans Gully Beds|33330|6|Mentioned|p171|||Time-equivalent.||||||
27742|Chinamans Gully Beds|34295|6|Mentioned|p34|||Eocene||||||
27742|Chinamans Gully Beds|34308|6|Mentioned|p192|||Separates Blanche Point Marls & Port Willunga Beds||||||
27742|Chinamans Gully Beds|35542|6|Mentioned|p4|||Refers Reynolds(1953). Misspelling of Chinaman Gully.||||||
27742|Chinamans Gully Beds|35689|6|Mentioned|p19|||Refers Reynolds(1953). Misspelling of Chinaman Gully.||||||
27742|Chinamans Gully Beds|38621|6|Mentioned|Table 1|||Refers Reynolds  1953.||||||
27742|Chinamans Gully Beds|40442|4|Described|p27|||||||||
82100|Chinmina syenite|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Coulta/Cleve domains.|c. 1700 Ma|Moody suite||||
24841|Chitalanga Volcanics|35078|6|Mentioned|p257|||||||||
39960|Chocolate Series|24195|6|Mentioned|p43|||||||||
32545|Christie's Beach beds|44199|14|Not recorded|p596|Quaternary|Neogene|Age late Tertiary-Quaternary.||||||
35824|Christmas Rocks granite|23317|6|Mentioned|378|||||||||
69762|Claude Hills peridotite/gabbro intrusion|44109|5|Briefly described|p10, p44|Mesoproterozoic|Mesoproterozoic|Informal name for part of the Giles Complex mafic-ultramafic intrusions. Detailed lithology presented. Within the Blackstone-Jameson region.||||||
69762|Claude Hills peridotite/gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name.  Poorly exposed thin sliver of altered peridotite, pyroxenite and gabbro.||||||
79548|Cleve Group""|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.||||||
28283|Cleve Metamorphics|23818|5|Briefly described|p27 Fig.6|||Max. thickness:>30 000 ft. Geological Province: Gawler Block.||||||
28283|Cleve Metamorphics|29838|6|Mentioned|p7|||||||||
28283|Cleve Metamorphics|30922|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian||||||
28283|Cleve Metamorphics|31034|6|Mentioned|p127|||Also mention P129||||||
28283|Cleve Metamorphics|31320|5|Briefly described|p13|||Lower Proterozoic.||||||28-FEB-08
28283|Cleve Metamorphics|31923|6|Mentioned|p5|||||||||
28283|Cleve Metamorphics|32427|5|Briefly described|p9|||Precambrian.||||||28-FEB-08
28283|Cleve Metamorphics|32428|6|Mentioned|p99|||||||||
28283|Cleve Metamorphics|32429|6|Mentioned|p92|||||||||
28283|Cleve Metamorphics|32434|6|Mentioned|p103|||||||||
28283|Cleve Metamorphics|32435|6|Mentioned|p111|||||||||
28283|Cleve Metamorphics|32436|6|Mentioned|p120|||||||||
28283|Cleve Metamorphics|32437|6|Mentioned|p12|||||||||
28283|Cleve Metamorphics|32440|6|Mentioned|p110|||||||||
28283|Cleve Metamorphics|32507|6|Mentioned|Table 3|||||||||
28283|Cleve Metamorphics|33055|6|Mentioned|p14|||||||||
28283|Cleve Metamorphics|33224|6|Mentioned|p43|||||||||
28283|Cleve Metamorphics|33468|4|Described|p201|||Correlates with Mt Bruce Supergroup. See also p204||||||28-FEB-08
28283|Cleve Metamorphics|33470|4|Described|p461|||||||||
28283|Cleve Metamorphics|33472|6|Mentioned|p470|||||||||
28283|Cleve Metamorphics|33479|6|Mentioned|p18|||||||||
28283|Cleve Metamorphics|33557|6|Mentioned|p10|||Refers Thomson (1968)||||||
28283|Cleve Metamorphics|33727|6|Mentioned|p35|||Refs. Thomson(1969).||||||
28283|Cleve Metamorphics|34537|4|Described|p28|||Lower Proterozoic.||||||28-FEB-08
28283|Cleve Metamorphics|34685|6|Mentioned|p353|||||||||
28283|Cleve Metamorphics|34718|6|Mentioned|p13|||||||||
28283|Cleve Metamorphics|34933|5|Briefly described|p58|||||||||
28283|Cleve Metamorphics|34941|6|Mentioned|p234|||||||||
28283|Cleve Metamorphics|34957|5|Briefly described|p395|||||||||
28283|Cleve Metamorphics|35003|6|Mentioned|p121|||||||||
28283|Cleve Metamorphics|35021|6|Mentioned|p157|||||||||
28283|Cleve Metamorphics|35078|6|Mentioned|p257|||||||||
28283|Cleve Metamorphics|35130|6|Mentioned|p7|||||||||
28283|Cleve Metamorphics|35255|6|Mentioned|p7|||||||||
28283|Cleve Metamorphics|35565|6|Mentioned|p16|||Base metal program.||||||
28283|Cleve Metamorphics|35676|6|Mentioned|Fig.2|||Regional geology.||||||
28283|Cleve Metamorphics|35772|4|Described|Table 1|||||||||
28283|Cleve Metamorphics|36003|5|Briefly described|p1027|||||||||
28283|Cleve Metamorphics|36073|6|Mentioned|p330|||||||||
28283|Cleve Metamorphics|38068|5|Briefly described|p66|||||||||
28283|Cleve Metamorphics|38404|6|Mentioned|p16|||||||||
28283|Cleve Metamorphics|38969|6|Mentioned|p198|||||||||
28283|Cleve Metamorphics|41995|6|Mentioned|p17|||||||||
28283|Cleve Metamorphics|43052|6|Mentioned|p51|||Refers to Thomson (1969).||||||28-FEB-08
28283|Cleve Metamorphics|44660|14|Not recorded|map legend||Carpentarian|Carpentarian, lithology.||||||
28283|Cleve Metamorphics|44864|5|Briefly described|Map Legend||Carpentarian|||||||
77795|Cleve Metamorphics""|68208|6|Mentioned|p32|||Of Dalgarno et al (1968) included what is now distinguished as Cooyerdoo Granite.||||||
82953|Cleve Subgroup|72484|6|Mentioned|p2|||||Hutchison Group.||||
80269|Cliffton Formation|71266|6|Mentioned|p614 Fig.3|Miocene|Oligocene|Otway Basin.||||||
34283|Colbert Granitoid Suite|22690|5|Briefly described|P305||Statherian|Age of unit is 1757+/-14 Ma||||||
34283|Colbert Granitoid Suite|24526|5|Briefly described|p98|Paleoproterozoic|Paleoproterozoic|Part of the Lincoln Batholith.  Granite, charnockite and gabbro-norite.  Age: 1846+/-14Ma.  Probably correlates with Minbrie Gneiss.||||||07-NOV-08
34283|Colbert Granitoid Suite|61307|5|Briefly described|p37|Paleoproterozoic|Paleoproterozoic|Hornblende-biotite rocks. Age: 1853+/-4Ma.||||||07-NOV-08
27992|Colbert Suite|22629|6|Mentioned|p157|Proterozoic|Proterozoic|||||||
27992|Colbert Suite|43052|4|Described|p81,Table 4.4|||||||||05-MAR-08
27992|Colbert Suite|50605|5|Briefly described|p(i), 3.1, 5.2|||Geological Province: Gawler Craton and Curnamona Province. Of the Younger Lincoln Supersuite.||||||05-MAR-08
27992|Colbert Suite|61307|5|Briefly described|p39 Fig. 19|||Abbreviated version of Colbert Granitoid Suite. ||||||
27992|Colbert Suite|64131|6|Mentioned|p1409|||Associated with Kimban orogeny.|||||Felsic plutons.|
27992|Colbert Suite|64313|6|Mentioned|p450|Paleoproterozoic|Paleoproterozoic|Name abandoned and rocks now referred to as Colbert Granite.||||||09-FEB-10
27992|Colbert Suite|65376|6|Mentioned|p65.|||Name replaced by Colbert Granite.||||||
67945|Colville Formation|44133|6|Mentioned|p184|||||||||
30090|Composite Gneiss Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
30090|Composite Gneiss Suite|23248|5|Briefly described|Fig2p169|||||||||
30090|Composite Gneiss Suite|23869|5|Briefly described|p13|||Not a formal name.||||||
30090|Composite Gneiss Suite|43086|5|Briefly described|p2|||Not to be viewed as a strict stratigraphic unit.||||||
30090|Composite Gneiss Suite|63519|5|Briefly described|p10 Fig. 3|||Geological Province: Olary Block.||||||11-JUN-08
30090|Composite Gneiss Suite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Olary Domain. Informal name.||Unit in Willyama Supergroup.||Is overlain by Quartzo-feldspathic Suite.||
30090|Composite Gneiss Suite|70657|5|Briefly described|p25, p77|||Clarke et al. (1986), for extensive areas of quartzofeldspathic composite gneiss and migmatite. Suggested in this study that the name not be used in a stratigraphic sense; Morialpa Migmatite instead. Appears on p77 to be part-equivalent to Curnamona Group.||||||
78309|Compton Sandstone|68211|5|Briefly described|p28, p29|||Trade name only - produced from the Gambier Limestone. Iron oxide staining contributes to the rock's colour. Durable stone with high-density, low water absorbtion and moderate strength.|||||Comprises pale reddish beige, fairly homogeneous dolomite, massive to vaguely macro-layered, medium-grained crystalline with minor porosity.|
82101|Con Bore granite|72459|5|Briefly described|p64, p86-89, p94-99|Mesoproterozoic|Mesoproterozoic|Geochemically identical to the Golden Pole granite and is interpreted to represent the same unit on opposite ends of a fold. Therefore the authors recommend Con Bore granite be discontinued and outcrops instead be referred to as Golden Pole granite.||Moolawatana Suite||||17-NOV-20
67946|Condowie Silt Member|44133|5|Briefly described|p164, 152 Fig. 10.2|Oligocene|Eocene|Of the Clinton Formation. Geological Province: Saint Vincent Basin. Thickness: 20m.||||||
83521|Coober Pedy Metamorphics|73155|6|Mentioned|p277, p284-285|||Gawler Craton. Similar lithology to Skylark Metamorphics but with more extensive reworking in Kararan Orogeny.||||||05-SEP-22
78885|Coober Pedy Ridge Paragneisses|62641|6|Mentioned|p277 Fig.1. |||Gawler Craton basement geology.||||||20-MAY-14
78885|Coober Pedy Ridge Paragneisses|69004|6|Mentioned|p18|||Gawler Craton.||||||
75399|Coober Pedy Ridge metasediments|65390|6|Mentioned|p22 Fig. 3||Statherian|Coober Pedy Domain, Gawler Craton. Also called Coober Pedy Ridge paragneisses. Age of <1750 Ma given.||||||
38532|Coober Pedy Ridge paragneisses|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
38532|Coober Pedy Ridge paragneisses|24505|5|Briefly described|p5 Fig. 1|||Informal name. Geological Province: Gawler Craton.||||||19-MAY-14
38532|Coober Pedy Ridge paragneisses|60515|6|Mentioned|p116 Fig.1 |||||||||
38532|Coober Pedy Ridge paragneisses|61522|5|Briefly described|p5 Fig.1|||Informal name. Geological Province: Gawler Craton.||||||
38532|Coober Pedy Ridge paragneisses|64722|6|Mentioned|Fig. 5 p.13|Mesoproterozoic|Mesoproterozoic|Informal name. Of South Australian Craton.||||||
38532|Coober Pedy Ridge paragneisses|64739|6|Mentioned|p264 Fig.1.|Mesoproterozoic|Mesoproterozoic|Gawler Craton. Informal name.||||||
38532|Coober Pedy Ridge paragneisses|65376|6|Mentioned|p8 Fig.1.1, pp218-223.||||Protolith c.1750 Ma; metamorphism 1589 +/- 11 Ma.|||||
38532|Coober Pedy Ridge paragneisses|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
38532|Coober Pedy Ridge paragneisses|66302|6|Mentioned|p4 Fig.3, |||Coober Pedy Domain, Gawler Craton. Also referred to as the Coober Pedy Ridge metasediments on p32. ||||||
38532|Coober Pedy Ridge paragneisses|69649|6|Mentioned|p6 Fig.4,|||||||||
75613|Coobowie Limestone (SA2)|63222|5|Briefly described|p40|Miocene|Miocene|Age: 20-15Ma. Fine-grained, cream to white, flat-lying, fossiliferous. Correlated with Port Willunga Formation. Marketed as the dimension stone Yorke Peninsula Limestone.||||||
83509|Coodnambanna Metaconglomerate|73155|5|Briefly described|p266, p282 Fig.13, p283, p285|||Mount Woods Domain, southern. Exposed in small area at Spire Hills, immediately underlying quartzite has a maximum depositional age of 1725 Ma (O'Sullivan, 2010). 1590 +/- 10 Ma age of metamorphic zircon rims constrains timing of high-grade metamorphism. See also Coodnambana Metaconglomerate, p265.||Mount Woods Complex||Unconformably overlies Skylark Metasediments.||
33229|Cooks Gap Schist|44660|14|Not recorded|map legend||Paleoproterozoic|L.Proterozoic, lithology.||||||07-NOV-08
78809|Cooladding Granite|64137|6|Mentioned|p1553 Fig.8|||Neodymium isotope data.||||||
81617|Coomandook Limestone|70029|6|Mentioned|p153,165|Neogene|Neogene|||||Overlain unconformably by Bridgewater Formation.||
23507|Coombes Springs Formation|38682|6|Mentioned|Fig.3|||||||||
23507|Coombes Springs Formation|39804|2|Defined|p165|Quaternary|Quaternary|Correct spelling is Coomb||||||
67938|Coonigan Formation, lower|44133|6|Mentioned|p28|||Informal, see Coonigan Formation.||||||
34548|Coorana Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
34548|Coorana Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Lochkovian|Of the Curdimurka Subgroup (Callanna Group).||||||
24874|Coorikiana Sandstone""|41086|5|Briefly described|p99|||||||||
24874|Coorikiana Sandstone""|41523|6|Mentioned|p277|||||||||
42500|Coorong carbonate sediments|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Otway Basin.||||||
75512|Cooyerdoo granite|65221|5|Briefly described|p26, 27, p28 Fig.3|Mesoarchaean|Mesoarchaean|c.3150 Ma. Informal name. Granitic gneiss||||||21-SEP-09
34746|Copa Member|12796|5|Briefly described|p456 Fig. 2|Turonian|Turonian|Of the Waarre Formation (Sherbrook Group). Geological Province: Otway Basin/Gambier Embayment.||||||
34746|Copa Member|22470|5|Briefly described|p13 Fig. 17|Turonian|Turonian|Of Waarre Formation, Sherbrook Group.||||||
81540|Cordilla Silcrete|71415|6|Mentioned|p11|Neogene|Paleogene|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||||||
70596|Cordillo Silcrete""|61825|5|Briefly described|p138|Oligocene|Late Eocene|See also "Cordillo Surface". Both of Wopfner and Twidale (1967) and Alley (1998). Geological Province:  Lake Eyre Basin.||||||
38352|Corny Point augen gneiss""|23803|6|Mentioned|p33|||Informal name -  unpublished Webb (1978).||||||
39962|Corraberra Sandstone Member""|24195|6|Mentioned|p44,47|||Informal name of the Corraberra Sandstone Member. Parent: Tent Hill Formation||||||
34789|Corrodgerie Formation|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
72307|Corrodgery formation|23981|6|Mentioned|p23|||Informal - see Corrodgery Formation.||||||
81273|Corundum Creek Schist member|68205|5|Briefly described|p85|||Geological province: Curnamona Province.||Unit of Radium Creek Metamorphics.|||Corundum-bearing biotite schists and phlogopitites; biotite- or phlogopite-rich corundum-, spinel- and sapphirine-bearing rocks.|
36881|Corundum Greek Schist Member|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
80388|Corunna Group|71242|14|Not recorded|p9|||Of Miles (1954). Name no longer used.|||Included Lincoln Gap Flagstones, Tregalana Shales.|||07-FEB-18
80390|Corunna Range Rudaceous and Arenaceous Formation""|71242|14|Not recorded|p9|||Of Mawson (1947). Correlated with Tent Hill Formation, "Emeroo Range Basal Rudaceous and Arenaceous Formation".||||||
80274|Coulta granodiorite|71341|6|Mentioned|p188 fig 7|||||||||
76823|Cox Sandstone|67030|6|Mentioned|p409 Fig. 2|Cryogenian|Cryogenian|||Farina Subgroup||Overlies the Tapley Hill Formation, ?underlies and ?is equivalent to the Tarcowie Siltstone.||26-APR-12
67939|Crayfish Formation""|44133|6|Mentioned|p144|||Used for some Pretty Hill Formation equivalents in SA.||||||
69948|Crayfish Group, upper|22686|5|Briefly described|p745|||Includes the Katnook Sandstone.  Geological Province: Otway Basin.||||||
73540|Crayfish Member|63124|6|Mentioned|p93|||Probably misspelt? Regarded by the authors as an equivalent to the Naracoorte Limestone Member of the Gambier Limestone.||||||18-FEB-08
40267|Crayfish subgroup|23911|6|Mentioned|p98|||Informal-see Crayfish Subgroup.||||||
82027|Crocker Well Diorites|72454|6|Mentioned|p2 Fig.2, p25 Tb.4, p61, p63-65 Tb. A3|Mesoproterozoic|Mesoproterozoic|Part of the Olary Domain. Geochronology by conventional U-Pb Ludwig and Cooper (1984). Shown as Crocker Well diorites p17, p25, 35, 48. May be accidently formalised in figures and tables.|1567 +/- 66 Ma.|||Coeval with Crocker Well Suite|Includes diorites.|
35402|Crockers Well Granite|23210|6|Mentioned|p26|||Contains Wollastonite hosted in skarns.||||||
35402|Crockers Well Granite|65455|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Curnamona Province.||Bimbowrie Suite.|||A highly alkaline granite which exhibits elevated U contents.|09-MAY-12
75185|Crockers Well Suite|62592|5|Briefly described|p18, p45.|||S-type. Large enclaves of Willyama Supergroup metasediments are often preserved, but with varying degrees of ingestion.||Unit in Ninnerie Supersuite.|||Biotite granite.|
75185|Crockers Well Suite|63866|5|Briefly described|p42|||||Ninnerie Supersuite|||S-type granites.|
75185|Crockers Well Suite|64741|5|Briefly described|p313|||Of the Ninnerie Supersuite (1590-1580Ma). Dominantly biotite-rich and sodic varieties, which include trondhjemite, alaskite and more mafic I-type granodiorite and diorite.||||||07-FEB-11
81681|Crockers Well Suite''|63102|6|Mentioned|p42|||Geological province: Olary Domain, Curnamona Province. Biotite and sodic granites of the Crockers Well - Billeroo region (Barovich and Foden, 2002).||||||
41674|Crockers Well adamellite|50605|5|Briefly described|p9.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary 1590Ma Supersuite. Age: 1578-1579 +/- 2.7Ma (U-Pb).||||||
41675|Crockers Well alaskite|50605|5|Briefly described|p9.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary 1590Ma Supersuite. Age: 1580 +/- 21Ma (U-Pb).||||||
39298|Crockers Well granitoids|24289|6|Mentioned|p47|||Not intended as a formal name.||||||
41676|Crockers Well leucoadamellite|50605|5|Briefly described|p9.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary 1590Ma Supersuite. Age: 1578-1570 +/- 10Ma (U-Pb).||||||
26506|Cultana Complex|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26506|Cultana Complex|65483|6|Mentioned|p19|||Informal name of Geological Survey of SA (1983). Superseded by Cultana Subsuite.||||||
82477|Cultana Suite|72949|6|Mentioned|p36|Calymmian|Calymmian|Olympic Domain, south. Yorke Peninsula / Eastern Eyre Peninsula. I-type granites.|1584 +/- 3 Ma|||||
76831|Cunyarie Rocks Granite|67028|6|Mentioned|p362|Calymmian|Calymmian|Incomplete name used in Table 1 p364 where information on magnetic characteristics presented. Described as Roxby Downs-type p362, p364, but shown as Kokatha-type in Table 1. See also informal Cunyarie Rocks granite, p373.||Hiltaba Suite Granitoids||||24-APR-12
76832|Cunyarie Rocks granite|67028|6|Mentioned|p373|||Mis-spelling of Cunyarie Rocks Granite.||||||24-APR-12
69713|Curdie Group|23830|5|Briefly described|Fig. 6|Late Cretaceous|Late Cretaceous|Geological Province: Gambier Embayment, Otway Basin.||||||12-SEP-05
70619|Curnamona metabasites|62373|5|Briefly described|p511|||Informal term for a suite metabasites in the southern Curnamona Province, with informal group names such as Mingary, Mundi, Outalpa, Plumbago, Waukaloo and Weekeroo which are informal nomenclature.||||||
82476|Cusin Creek pluton|62536|4|Described|p639, 641-642, 655-657|||Structure and age discussed.|1596 +/- 3 Ma.||Broken Hill area. Igneous crystallisation age.|Intrudes Paragon Group, Bijerkerno Metasediments.|A lozenge-shaped, medium-grained, nonporphyritic, muscovite-biotite granitoid body.|
82476|Cusin Creek pluton|72949|6|Mentioned|p36|Calymmian|Calymmian|[Informal unit name?]. Curnamona Province. Broken Hill / Olary Blocks.|1596 +/- 3 Ma|||||
80292|Cuttapirrie beds|71342|5|Briefly described|Ch5 p10|||Obsolete name, superseded by the Poolowanna Formation. ||||||
67940|Cuttapirrie beds""|44133|5|Briefly described|p105 |Jurassic|Jurassic|Now known as the Poolowanna Formation.||||||
67940|Cuttapirrie beds""|69946|5|Briefly described|p10|||Refers to a claystone, siltstone and sand unit in the interval 2422 - 2476m in Cuttapirrie 1. It has also been referred to as Poolowanna Formation. In this work the authors name it the Poolowanna facies, a silty and coaly facies of the Hutton Sandstone.||||||
29676|Daralingee beds|42999|5|Briefly described|Table 2,p90|Late Permian|Early Permian|Misspelling of Daralingie Formation.||||||
74069|Daralingie Group|60717|6|Mentioned|p40|||Appears as Daralingie Formation in Figure 2 (same page) - probably mis-named? Geological Province: Cooper Basin.||||||18-FEB-08
83176|Dark Peake Group|73122|6|Mentioned|p19|Palaeoproterozoic|Palaeoproterozoic|Mis-spelling of Darke Peak Group.||||||
79549|Darke Peake Group""|69048|6|Mentioned|p3|||Central-western Eyre Peninsula.|c.1875 Ma.|||||
82954|Darke Peake Subgroup|72484|6|Mentioned|p2|||Basement to Middleback Ranges area of Gawler Craton.||Hutchison Group.||||
34209|Davies Bore Conglomerate|22650|6|Mentioned|p 159|||Age - Cambrian p 159.  Province - Officer Basin.||||||
39578|Dawsley Andalusite Beds|24465|5|Briefly described|p346 Fig.3|||Of Mirams, 1962 - of the Brukunga Formation.  Probably obsolete.||||||19-JAN-05
39579|Dawsley Pyrite Beds|24465|5|Briefly described|p346 Fig.3|||Of Mirams, 1962. Probably superseded.||||||
81684|Dayanna Formation|63102|4|Described|p14,33,36-37|||Geological province: Olary Domain, Curnamona Province. Occurs in the core of the Mount Howden Syncline. Formerly the Dayanna Pelite.||Unit of Mount Howden Subgroup.||Equivalent to Dalnit Bore Metasediments.|Pale grey silky, andalusite and staurolite-bearing schist.|22-OCT-19
81684|Dayanna Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Mount Howden Subgroup.||||
83532|Deuter Granite|73525|5|Briefly described|p19 Fig.13|Statherian|Statherian|Spencer Domain.|1742+/-6 Ma crystallisation age|Moola Suite|||Felsic intrusive.|
76213|Devil's Playground Volcanics|66520|6|Mentioned|p9.|||Informal name;  now defined as Devils Playground Volcanics.||||||
76213|Devil's Playground Volcanics|67058|5|Briefly described|p476, p493.|Neoarchean|Neoarchean|Central Gawler Craton. The formal name does not have the apostrophe.||||||15-MAR-12
76213|Devil's Playground Volcanics|71859|5|Briefly described|p2, p28|Neoarchean|Neoarchean|Central-western Gawler Craton.|c. 2555 Ma|Mulgathing Complex.||||
76213|Devil's Playground Volcanics|73155|6|Mentioned|p283|Neoarchean|Neoarchean|Possible correlate of Danae Hill Metavolcanics.|ca. 2558 Ma|||||
81860|Devil's Playground volcanics|68128|5|Briefly described|p5|||Gawler Craton. Informal name. Probably misspelt. See also Devils Playground Volcanics p6, p7, Devils Playground volcanics  Table 2 p6.|2553 +/- 9 Ma (ID-TIMS U-Pb)||||Weakly metamorphosed acid volcanics.|
34764|Dey Dey Mudstone|22922|5|Briefly described|34|||Parent Ungoolya Group||||||
34764|Dey Dey Mudstone|23282|2|Defined|p59||Neoproterozoic|Informally introduced by Sukanata (1993) and formalised by Zang (1995) who informally subdivided into lower and upper. Previously known as lower "Ungoolya Formation' & lower Rodda beds. Age: Precambrian, Neoproterozoic, mid Marinoan Epoch. of Ungoolya Gp.||||||
34764|Dey Dey Mudstone|24112|5|Briefly described|p254 Fig.2, p268 Tb.5|Neoproterozoic|Neoproterozoic|Of the Ungoolya Group. Geological Province: Officer Basin||||||
34764|Dey Dey Mudstone|24476|6|Mentioned|p546|||Formerly the Rodda beds. Geological Province: Officer Basin.||||||
34764|Dey Dey Mudstone|50127|6|Mentioned|p47, p48 Fig.2|||Geological Province: Officer Basin||||||
34764|Dey Dey Mudstone|61560|5|Briefly described|p498 Tb. 4|||Contains confirmed Acraman impact ejecta. Geological Province: central Officer Basin.  See also p500. ||||||
34764|Dey Dey Mudstone|61565|5|Briefly described|p611|||Supersedes Rodda beds. Contains ejecta bands related to the Acraman-Bunyeroo impact event in drillcores. Geological Province: Adelaide Fold belt.||||||20-APR-06
34764|Dey Dey Mudstone|61732|3|Fully described|p5 Tb. 1, p60-61|Cryogenian|Cryogenian|Of Ungoolya Group. Previously referred to as "lower Rodda beds" (Brewer et al 1987; Thomas 1990). Overlies Murnaroo Fm; unconformably overlain by Narana Fm. Geol.Prov: Officer Basin. See also p58 Fig. 22, p145 Fig. 51.||||||07-FEB-11
34764|Dey Dey Mudstone|63811|5|Briefly described|p500-502, Fig 2, p505, p523-528 App A|Ediacaran|Ediacaran|86 m thick in Giles 1 (Officer Basin). Up to 900 m thick elsewhere. Contains acritach species.||Basal unit of the Ungoolya Group.||Overlain by Karlaya Limestone.|Upper unit laminated dolomitic or calcareous silt and mudstone. Lower unit red-brown to green-gray silty mudstone.|04-SEP-14
34764|Dey Dey Mudstone|64794|4|Described|p244-245, p248, p251-8, p272-273|Ediacaran|Ediacaran|See also p238 fig 2, p241 Tb.1, p242 fig 3. Contains impact ejecta (perhaps Acraman Impact) within shale near base. Preservation of palynomorphs improves upwards through the unit.||Ungoolya Group||Overlies Murnaroo Formation (conformably). Overlain conformably by Karlaya Limestone.|Basal 123m thick uniform red-brown slightly fissile mudstone. Upper 175m dark grey-green parallel-laminated dolomitic or calcareous siltstone, and rhythmically interlaminated very fine sandstone and siltstone; includes an organic-rich shale horizon.|
34764|Dey Dey Mudstone|64797|6|Mentioned|p153 Fig.2|Ediacaran|Ediacaran|Officer Basin. Lithology/rank not shown on diagram.||||||
34764|Dey Dey Mudstone|66569|4|Described|p859, p860, p861 fig.2,|Ediacaran|Ediacaran|Correlated with Bunyeroo Formation; contains an Acraman impact ejecta horizon; lower part red brown mudstone with graded siltstone-mudstone laminae; of Ungoolya Group; unconformably underlies Karlaya Limestone; unconformably overlies Murnaroo Sandstone.||||||
34764|Dey Dey Mudstone|67912|5|Briefly described|p12-14, 16, 24-27|Ediacaran|Ediacaran|Officer Basin. Acanthomorphic acritarchs occur in Lake Maurice West 1 drillhole where it is 169.7m thick. Over 900m thick in the Munyarai Trough. Prodelta to shelf environments. Lithostratigraphic column with taxa and revised biozones. Numerous photomicrographs.||Ungoolya Group.||Overlies Murnaroo Formation. Is overlain conformably and transitionally by Karlaya Limestone. Includes the Acraman impact ejecta layer.|A lower unit of massive to laminated, red-brown to green-grey silty mudstone, separated by a bed of dolomitic intraclasts from the upper unit of massive to laminated dolomitic siltstone to mudstone.|
34764|Dey Dey Mudstone|68030|6|Mentioned|p238|||Officer Basin. Can be correlated to the Bunyeroo Formation via regionally extensive Bunyeroo red beds bolide impact debris layer/chronostratigraphic marker, termed Acraman horizon in text on p238.||||||
34764|Dey Dey Mudstone|68269|5|Briefly described|p673-674|Ediacaran|Ediacaran|Officer Basin, eastern. c. 200-600 m thick. Lower portion contains a distal Acraman impact ejecta horizon that has a maximum thickness of 7 mm; serves as a marker horizon. Contains siltstone (till) pellets dispersed by floating ice. This lower interval also coincides with a major change in palynoflora.||Ungoolya Group||Unconformably underlain by Murnaroo Sandstone. Unconformably overlain by Karlaya Limestone. Correlates to Bunyeroo Formation.|Red brown mudstone with graded siltstone-mudstone laminae.|
34764|Dey Dey Mudstone|68274|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|||||||
34764|Dey Dey Mudstone|72478|6|Mentioned|p8|Marinoan|Marinoan|Officer Basin.|c. 600 Ma-590 Ma|Ungoolya Group||Overlies the Murnaroo Formation. Underlies the Karlaya Limestone.||24-MAR-21
34764|Dey Dey Mudstone|73099|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Officer Basin.||Ungoolya Group.||Overlies Murnaroo Formation. Is overlain by Karlaya Limestone.|Brown, reddish and grey, laminated, micaceous, clayey siltstone with interbeds of very fine- to very coarse-grained silty sandstone and granule conglomerate.|
77507|Diamond Bog dolomite|62537|6|Mentioned|p191 Fig.2. |Middle Cambrian|Middle Cambrian|Warburton Basin.||||Is overlain by Kalladeina Formation.||
78563|Dillingari Group|68731|6|Mentioned|p170 Fig 3.83|||Misspelt. See also Dullingari Group same page.||||||17-DEC-13
73541|Dilwyn "Clay"|63124|6|Mentioned|p89|||Of Baker (1953). Also known as "Dartmoor Formation" at the same time. Superseded by Dilwyn Formation. ||||||
41680|Donington Granitoid Supersuite|24197|6|Mentioned|p72|||Same as the Donington Suite? Age: ~1840-1820Ma.||||||07-FEB-11
41680|Donington Granitoid Supersuite|50605|5|Briefly described|p1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: ~1840-1820Ma.||||||07-NOV-08
68956|Donington Suite granitoids|61070|6|Mentioned|Map Legend|||||||||12-JAN-10
68956|Donington Suite granitoids|61725|5|Briefly described|p887, p890|Paleoproterozoic|Paleoproterozoic|Informal - refers to granite rocks of the Donington Suite. Age: 1.85Ga.||||||07-NOV-08
68956|Donington Suite granitoids|62729|5|Briefly described|p39 Fig. 1b, p40|Paleoproterozoic|Paleoproterozoic|Age: ~1850 Ma. Informal name - see Donington Suite. Geological Province: Gawler Craton.||||||07-NOV-08
68057|Donnington Granitoid Suite|24526|5|Briefly described|p98|Paleoproterozoic|Paleoproterozoic|Part of the Lincoln Batholith.  Granite, charnockite and gabbro-norite.  Age: 1850+/-1Ma.  Probably correlates with the Minbrie Gneiss.||||||07-NOV-08
68057|Donnington Granitoid Suite|61307|5|Briefly described|p37|||Voluminous charnockitic unit consisting of foliated mafic-felsic pyroxene to hornblende-biotite bearing megacrystic and even-grained gneisses. Geological Province: Gawler Craton.||||||27-MAY-08
68057|Donnington Granitoid Suite|63102|6|Mentioned|p36|||Geological province: Olary Domain, Curnamona Province.||||||
68057|Donnington Granitoid Suite|64828|6|Mentioned|p1067|||Misspelt - see Donington Granitoid Suite.||||||04-MAR-09
68057|Donnington Granitoid Suite|65376|6|Mentioned|p54. |||See Donington Suite.||||||
68057|Donnington Granitoid Suite|74367|6|Mentioned|p4|Orosirian|Orosirian|Gawler Craton.|1850-1840 Ma|||||
77402|Donnington Suite|62641|6|Mentioned|p277 Fig.1. |||[Mis-spelling of Donington]. See also references to Donington Granitoid Suite (p278, p285).|1.85 Ga.|||||
77402|Donnington Suite|65376|6|Mentioned|p92 Fig. 2.82. |||Mis-spelling of Donington Suite.||||||
77402|Donnington Suite|69213|6|Mentioned|p28 Fig.|||Eyre Peninsula. Includes migmatised orthogneisses.||||||
34320|Doora Metasediments|22629|6|Mentioned|p152, fig2p147|Paleoproterozoic|Paleoproterozoic|Expected to be revised. Describes the same unit as Doora Schist||||||07-NOV-08
34320|Doora Metasediments|24475|5|Briefly described|p46, p50|||Orginally named Doora Schist, now Doora Member of Wandearah Formation.||||||
34320|Doora Metasediments|50605|5|Briefly described|p8.7|||Of the Wallaroo Group. Geological Province: Gawler Craton & Curnamona Province.||||||
34320|Doora Metasediments|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34320|Doora Metasediments|65375|6|Mentioned|p21.|||Named by Conor (1995); formerly Doora Schist (Parker 1980); superseded by Doora Member.||||||
34320|Doora Metasediments|65390|5|Briefly described|p18, p23 Fig.3|Statherian|Statherian|Of Wallaroo Group. See also Doora Schist (p10, p23 Fig. 3, p26 Tb. 1). Age of 1760 +/- 7 Ma from interbedded Moonta Volcanics.||||||
34320|Doora Metasediments|72461|6|Mentioned|p6|||Gawler Craton.||||||
37079|Doora Metasediments""|23719|6|Mentioned|p16|||Geological Province: Gawler Craton||||||
39179|Doora Porphyry Member|24475|6|Mentioned|p56|||Misspelt - see Doora Member.||||||
23554|Doora Schist|22629|6|Mentioned|fig2, p,152,158|Paleoproterozoic|Paleoproterozoic|Expected to be revised. Describing same unit as Doora Metasediments.||||||07-NOV-08
23554|Doora Schist|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
23554|Doora Schist|23719|4|Described|p16|Paleoproterozoic|Paleoproterozoic|See also page 16 Table 3. Age: 1741+/-9 Ma (U-Pb zircon). Of Wallaroo Group. Geological Province: Gawler Craton.||||||07-NOV-08
23554|Doora Schist|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
23554|Doora Schist|24362|6|Mentioned|p41|||||||||
23554|Doora Schist|24475|5|Briefly described|p46, p50|||Renamed Doora Metasediments, now superseded by Doora Member of Wandearah Formation.||||||
23554|Doora Schist|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
23554|Doora Schist|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23554|Doora Schist|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23554|Doora Schist|40644|6|Mentioned|p121, p129, p130|Mesoproterozoic|Mesoproterozoic|On Yorke Peninsula. Age: 1540-1440Ma.||||||13-AUG-08
23554|Doora Schist|41972|6|Mentioned|p366|||||||||
23554|Doora Schist|42167|5|Briefly described|p116|||||||||
23554|Doora Schist|42235|6|Mentioned|p134|||||||||
23554|Doora Schist|43052|5|Briefly described|p64|||||||||
23554|Doora Schist|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Schist, amphibolite, metavolcanics.||||||07-NOV-08
23554|Doora Schist|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23554|Doora Schist|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23554|Doora Schist|60515|6|Mentioned|p116 Fig.1 |||||||||
23554|Doora Schist|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
23554|Doora Schist|65375|6|Mentioned|p21.|||Named by Parker (1980);  superseded by Doora Metasediments (Conor 1995); later Doora Member.||||||
23554|Doora Schist|65376|6|Mentioned|p8 Fig.1.1, p101. |||Name replaced by Doora Member.||||||
23554|Doora Schist|65390|5|Briefly described|p10, p18, p26 Tb. 1|Statherian|Statherian|Of Wallaroo Group, Gawler Craton. See also Doora Metasediments. Interbedded Moonta Volcanics give U-Pb age of 1760 +/- 7 Ma. Intruded by Tickera Granite. Hosts Cu-Au mineralisation at Wheal Hughes.||||||26-FEB-15
23554|Doora Schist|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
23554|Doora Schist|66302|6|Mentioned|p4 Fig.3, p29, p33|||Olympic Domain, Gawler Craton. ||||||
23554|Doora Schist|69649|6|Mentioned|p6 Fig.4,|||||||||
82102|Doorah Metasediments|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic||c. 1760-1740 Ma|||||
40386|Doughboy breccia|24431|5|Briefly described|p189 Fig. 1|||Geological Province: Olary Domain.||||||
69580|Dry Creek Bluestone|61237|6|Mentioned|p36|||Informal name. From the grounds of the Yatala Labour Prison - historic building stone.||||||
70561|Dry Creek Bluestone""|61525|6|Mentioned|p41 (photo)|||Building stone. Informal name.||||||02-JUN-06
39199|Dry Creek Sands, upper|23768|5|Briefly described|p33|Late Pliocene||Informal - see Dry Creek Sands. See discussion p33.||||Correlated with Hallett Cove Sandstone, Norwest Bend Formation, Goodwood Formation||11-SEP-09
69667|Dry Creek Sandstone|61155|5|Briefly described|p17|Late Pliocene|Early Pliocene|See also Dry Creek Sands. Age: Partially overlain by and interfingers with Hallett Cove Sandstone; and, partially overlain by Carisbrooke Sand. Geological Province: St Vincent Basin.||||||
82041|Duddo Limestone Member|72445|5|Briefly described|App.7 p7.|Middle Miocene|Late Oligocene|Shown in App 7 Fig 4 and App6 as Duddo Limestone. Mentioned in text as thick limestone deposited in the far west of the Murray Basin.||Murray Group|||Shown as including limestone.|
25885|Duff Creek Beds|23054|5|Briefly described|p11|||||||||
25885|Duff Creek Beds|24175|6|Mentioned|p9|||Geological Province: Peake and Denison Inliers.||||||
25885|Duff Creek Beds|33468|6|Mentioned|p210|||Willouran ?||||||
25885|Duff Creek Beds|36733|2|Defined|p69|early Adelaidean|early Adelaidean|See also P33.||||||
25885|Duff Creek Beds|37854|6|Mentioned|p13|||||||||
25885|Duff Creek Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
25885|Duff Creek Beds|40294|6|Mentioned|p9|||See also Table 2||||||
25885|Duff Creek Beds|41403|5|Briefly described|p67|||||||||
25885|Duff Creek Beds|42238|6|Mentioned|p72|||||||||
25885|Duff Creek Beds|43052|5|Briefly described|p175,Table 6.2|||of Curdimurka Subgroup.||||||
25885|Duff Creek Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
25885|Duff Creek Beds|64796|6|Mentioned|p189 Fig.7, p195 Tb.3, p200-202|Neoproterozoic|Neoproterozoic|Appears in Fig.8 without the lithology; and as Duff Creek beds on p201.||Unit in Callanna Group.||||
67941|Dullingari Group, lower|44133|5|Briefly described|p34, 41|||Corresponds to Mount Chandler Sandstone.||||||
77508|Dullingarri group|62537|6|Mentioned|p191 Fig.2. |Late Cambrian|Middle Cambrian|Warburton Basin.||||||
78564|Dullinggari Group|68731|6|Mentioned|p170 Fig 3.83|Middle Ordovician|Cambrian|Misspelt. See also Dullingari Group same page..||||||17-DEC-13
73542|Dundas Volcanics|63124|6|Mentioned|p57|||||||||
23564|Dunns Mine Formation|36733|6|Mentioned|p31|||||||||
23564|Dunns Mine Formation|38108|6|Mentioned|Table 1|||||||||
23564|Dunns Mine Formation|41403|4|Described|p62|||||||||
34573|Dutton Diatreme|22830|6|Mentioned|P25|||||||||
29824|Dutton Metamorphics|43052|6|Mentioned|p51|||refers to Whitten (1966).||||||
29824|Dutton Metamorphics|61556|14|Not recorded|p10|Paleoproterozoic|Paleoproterozoic|||||||
78807|Ealbara Rhyodacite|64137|6|Mentioned|p1553 Fig.8 |||Neodymium isotope data from Stewart (1994) thesis. Shown as Ealbara/Carnding Rhy. in figure and only expanded [wrongly] in figure caption.||||||17-MAR-14
39159|East Kadina Group|24475|6|Mentioned|p51|||Informal name of Lynch (1982).||||||
39159|East Kadina Group|65375|6|Mentioned|p22.|||Not a recognised stratigraphic name. Used by Lunch (1982) for rocks in the New Cornwall Member of the Wandearah Formation.||||||
39158|East Kadina Group""|24475|6|Mentioned|p46|||Informal name of Lynch (1982).||||||
67942|Echidna beds""|44133|6|Mentioned|p139|||Superseded by Echidna Formation.||||||
77424|Edeowie Member|63569|6|Mentioned|p117 Fig.1|Early Cambrian|Early Cambrian|See Edeowie Limestone Member.||?of Billy Creek Formation.||||
77424|Edeowie Member|65925|6|Mentioned|p14 Fig.2.2.|Early Cambrian|Early Cambrian|Inadequate room in Figure 2 for this unit's full name: Edeowie Limestone Member.||||||
28525|Edeowie limestone|35395|6|Mentioned|p102|||||||||
29469|Edithburg Formation|42966|6|Mentioned|p179|||Yorke Peninsula. Correlated with Late Pliocene Norwest Bend Formation of Murray Basin and Wallaroo Formation, Yorke Peninsula.||||||23-AUG-18
81702|El Alamein Member''|71129|5|Briefly described|p109|Neoproterozoic|Neoproterozoic|Of Stuart Shelf. Local silty unit identified in some exploration reports overlying the Tassie Member.||Unit of Tapley Hill Formation.||Underlain by 'Tassie Member'.||21-OCT-19
24946|Elatina Sandstone|34534|6|Mentioned|Fig.2.13|||||||||
24946|Elatina Sandstone|72493|6|Mentioned|p43||||620 Ma.|||||
81703|Elizabeth Creek Conglomerate''|71129|5|Briefly described|p98,101|Tonian|Tonian|Of Stuart Shelf. Nomenclature from Mount Gunson Mines Pty Ltd (1975). Similar stratigraphic position to McLeay Beds and Moonlight Conglomerate. Interpreted to be Sturtian (early Neoproterozoic) in age, and possibly either a basal unit of Tapley Hill Formation (Thomson et al., 1976), or more recently interpreted to be part of Backy Point Formation (Mason et al., 1978, Cowley, 1991a).||||Partial equivalent to Backy Point Formation.||
80391|Emeroo Range Basal Rudaceous and Arenaceous Formation""|71242|14|Not recorded|p9|||Of Mawson (1947). Correlated with Tent Hill Formation, "Corunna Range Rudaceous and Arenaceous Formation". Regarded by Mawson as basal formation of the Adelaide "Series"||||||
68906|Emeroo sandstone|24138|5|Briefly described|p64|||Informal. See also Emeroo Quartzite. Geological Province: Adelaide Geosyncline.||||||
28533|Emu Bay Sandstone|30982|6|Mentioned|p435|||||||||
29923|Encounter Bay Granites|22848|6|Mentioned|35|||||||||
29923|Encounter Bay Granites|23023|6|Mentioned|p1799||Middle Cambrian|Max Age: 504 (+/-) 8 Ma.||||||
29923|Encounter Bay Granites|23869|5|Briefly described|p15 Fig. 3|Cambrian|Cambrian|||||||
29923|Encounter Bay Granites|43052|5|Briefly described|Fig.2.14|||||||||
29923|Encounter Bay Granites|43759|6|Mentioned|p446||Late Cambrian|||||||
29923|Encounter Bay Granites|44133|5|Briefly described|p51 Fig. 7.18, 55, 56 Table 7.3, 18|Ordovician|Cambrian|Megacrystic and even-grained granite. Age: 417-474Ma, 504 +/- 8Ma. I-Type to marginally S-Type. Of the Kanmantoo Group.||||||
29923|Encounter Bay Granites|63124|5|Briefly described|p51|||Probably should be Encounter Bay Granite. Age: 515-506Ma. In Victor Harbour.||||||
29923|Encounter Bay Granites|73188|6|Mentioned|p317|||Minerals record Rb-Sr and K-Ar isotopic disturbance from thermal events although whole-rock Rb-Sr does not.||||||
83512|Engenina Adamelite|73155|6|Mentioned|p265-266|Statherian|Statherian|Mount Woods Domain. Emplaced during late stages of Kimban Orogeny. Misspelling of Engenina Adamellite.|ca. 1692 Ma|Mount Woods Complex||Intrudes into Skylark Metasediments.||
76806|Engenina Ademallite|64726|6|Mentioned|p83 Fig.2.|||Mis-spelling of Adamellite.||||||
37126|Enorama Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
37126|Enorama Formation|66464|5|Briefly described|p167, p172-173 Figs.6-8|Cryogenian|Cryogenian|Adelaide Rift Complex. Basal shale marks major flooding surface, followed by a coarsening and shallowing upwards sequence. Overlain by Trezona Formation.||||||
37126|Enorama Formation|68030|6|Mentioned|p237|||Flinders Ranges.||||Overlain (locally disconformably) by Nuccaleena Formation.||
37126|Enorama Formation|68275|6|Mentioned|p59|||||||Overlies Etina Formation. Is overlain by Trezona Formation.||
37126|Enorama Formation|73255|6|Mentioned|p534 Fig.2|Cryogenian|Cryogenian|||||Overlies the Etina Fotmation, underlies the Trezona Formation.||
69474|Ernabella Adamellite suite|61154|6|Mentioned|p42 Appendix|||Of the Pitjantjatjara Supersuite in South Australia.||||||
36021|Ernabella Charnockite|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: 1180-1120Ma.  Geological Province: Musgrave Block.||||||
36021|Ernabella Charnockite|50607|5|Briefly described|p2.2|||Geological Province: Musgrave Block. Of the Kulgera Suite. See also Ernabella Adamellite.||||||
36021|Ernabella Charnockite|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||22-FEB-05
32776|Etadunna green arenaceous claystone|44228|14|Not recorded|p.131|||||||||
72297|Ethiudna psammopelite|62514|6|Mentioned|p747 Fig. 2|||Informal name for psammitic rocks of the Ethiudna Subgroup (Curnamona Group). Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
79791|Ettlewood Calc-silicate member|68126|6|Mentioned|p6|||Broken Hill Domain, Curnamona Province.||Broken Hill Group.||||
29440|Ettrick Marls|9124|5|Briefly described|Map Legend|Miocene|Oligocene|Glauconitic marls.||||||
29440|Ettrick Marls|42966|6|Mentioned|p122|||Synonym for Ettrick Formation.||||||
27269|Eucarro Dacite|22873|6|Mentioned|P10|||||||||
27269|Eucarro Dacite|24346|6|Mentioned|p111 App 1, p98 Fig.1|||Superseded by Eucarro Rhyolite Formation.||||||24-APR-12
27269|Eucarro Dacite|24474|5|Briefly described|p36 Fig. 1|||Of the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
27269|Eucarro Dacite|40430|2|Defined|p5|Mesoproterozoic|Mesoproterozoic|||||||
27269|Eucarro Dacite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
27269|Eucarro Dacite|42283|6|Mentioned|Fig.5 P82|||||||||
27269|Eucarro Dacite|42466|5|Briefly described|Map Legend|||||||||
27269|Eucarro Dacite|42475|4|Described|p16|||part of "younger" Gawler Range Volcanics||||||
27269|Eucarro Dacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
27269|Eucarro Dacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
27269|Eucarro Dacite|43052|5|Briefly described|p111|||of Gawler Range Volcanics||||||
27269|Eucarro Dacite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Gawler Range Volcanics. Acid volcanics.||||||26-MAY-05
27269|Eucarro Dacite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
27269|Eucarro Dacite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
27269|Eucarro Dacite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1592-1589Ma. Of the Lower Gawler Range Volcanics. Dacite to rhyolite, minor andesite and basalt.||||||
27269|Eucarro Dacite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Gawler Range Volcanics, Lower. Age: 1592-1589 Ma.||||||23-JUN-05
27269|Eucarro Dacite|65922|5|Briefly described|p17 Tb. 2, p18-19, 21|Calymmian|Calymmian|Of Gawler Range Volcanics. Subsequently included in Eucarro Rhyolite. Includes Poondanna Dacite Member. Conformably overlies Bittali Rhyolite and locally, Nonning Rhyodacite; underlies Yannabie Rhyodacite; intruded by Paney Rhyolite. Displays prominent columnar jointing and bold exposures. Chemically zoned from basal densely welded dacite (?rhyolite), through rhyodacite to dacite at the top. REE patterns imply common genesis with Yardea Dacite and Nonning Rhyodacite.||||||
27269|Eucarro Dacite|67028|5|Briefly described|p362, p364 Tb.1, p373|Calymmian|Calymmian|information on magnetic characteristics presented. Described as Roxby Downs-type p362, but shown as Kokatha-type in Table 1. See also Eucarro Rhyolite p366.||Gawler Range Volcanics||||24-APR-12
27269|Eucarro Dacite|69649|6|Mentioned|p17|Mesoproterozoic|Mesoproterozoic|||Unit in Gawler Range Volcanics.||||26-FEB-15
27269|Eucarro Dacite|72459|5|Briefly described|p17, p19, p46-47|Mesoproterozoic|Mesoproterozoic|Large volume unit interpreted to be ignimbritic in origin with minor interbedded lavas. Part of the 'mature' phase of the Gawler Range Volcanism.||Gawler Range Volcanics||||
38166|Eucarro Dacite""|24346|4|Described|p99, p98 Fig. 1|||Superseded by Eucarro Rhyolite which also includes the former "Nonning Rhyodacite", "Yannabie Rhodacite" and "Paney Rholite".  Parts also now included in Yardea Dacite. Of Gawler Range Volcanics.||||||
38633|Eucarro Rhyolite Formation|24346|3|Fully described|p111 Appendix 1|||Supersedes Eucarro Dacite and includes the former Yannabie and Nonning Rhyodacites and Paney Rhyolite (now Paney Rhyolite Member).  Referred to as Eucarro Rhyolite throughout text. Overlain by Yardea Dacite, underlain by Bittali Rhyolite.||||||24-APR-12
38633|Eucarro Rhyolite Formation|72065|6|Mentioned|p105|||Geological province: Gawler Craton. Informal/Misspelt use: See Eucarro Rhyolite.||Unit of Eucarro Rhyolite.||||
73536|Eumeralla Formation, Lower|61017|5|Briefly described|p6|||Informal - see Eumeralla Formation. Contains coal-bearing sediments in lower section of formation, considered the source for hydrocarbon play in Waarre Formation.||||||07-FEB-11
73536|Eumeralla Formation, Lower|63125|6|Mentioned|p116 Tb.7.6, p121 Tb. 7.11|||Informal - see Eumeralla Formation. Geological Province: Otway Basin||||||
73536|Eumeralla Formation, Lower|72050|6|Mentioned|p238|||One of the principal sealing units within the Crayfish Group plays.||||||
73536|Eumeralla Formation, Lower|73357|6|Mentioned|p43, p45, p47|Aptian|Barremian|Otway Basin. Correlated with the Pilosisporites notensis Spore-Pollen Zone of Morgan et al., (2002a), largely terrestrial palynofloras.||Of Otway Group.|Includes Windermere Sandstone.|Overlies Pretty Hill Formation, underlies Upper Eumeralla Formation.||
73537|Eumeralla Formation, Upper|63125|6|Mentioned|p121 Tb. 7.11|||Informal - see Eumeralla Formation. Geological Province: Otway Basin||||||
73537|Eumeralla Formation, Upper|73357|6|Mentioned|p43, p45, p47|Albian|Aptian|Otway Basin. Correlated with Crybelosporites striatus Spore-Pollen Zone and Coptospora paradoxa Zone, moderately frequent expression of brackish/marginal marine depositional environments. Uppermost part correlated to late Albian Phimopollenites pannosus Spore-Pollen Zone.||Of Otway Group.|Includes Heathfield Sandstone.|Overlies Lower Eumeralla Formation.||
73543|Eumeralla Formation, lower|63124|6|Mentioned|p70, p73|||Subdivisions of Kopsen and Scolefield 1990). Not generally accepted by industry and not in accordance with International Stratigraphic Guide. Informal name - see Eumeralla Formation.||||||
73544|Eumeralla Formation, middle|63124|6|Mentioned|p70|||Subdivisions of Kopsen and Scolefield 1990). Not generally accepted by industry and not in accordance with International Stratigraphic Guide. Informal name - see Eumeralla Formation.||||||
73545|Eumeralla Formation, upper|63124|6|Mentioned|p70|||Subdivisions of Kopsen and Scolefield 1990). Not generally accepted by industry and not in accordance with International Stratigraphic Guide. Informal name - see Eumeralla Formation.||||||
42359|Eurelia kimberlite|24364|6|Mentioned|p26|||Informal name. Diamondiferous rocks.||||||
42359|Eurelia kimberlite|71129|6|Mentioned|p136||||750+\-50 Ma|||||
42508|Everardian Granites|23818|6|Mentioned|p40 Fig.11|||Geological Province: Musgrave Block.||||||
69760|Ewarara pyroxenite intrusion|44109|4|Described|p10, p44|Mesoproterozoic|Mesoproterozoic|Informal part Giles Complex. Olivine bronzitite (or harzburgite), pyroxenite, melagabbro. Felsic granulite classified within the Mount Aloysius Complex (within the Giles Complex). Max. thick: >500m. ||||||
69760|Ewarara pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Bronzite, harzburgite, pyroxenite, melagabbro. Thickness: .500m.||||||21-SEP-05
24970|Eyre Formation""|40926|6|Mentioned|p22|||||||||
76214|Fabian Quartzite|67058|5|Briefly described|p479.|Paleoproterozoic|Paleoproterozoic|||Unit in Tarcoola Formation.||Overlies Peela Conglomerate.|Stromatolitic dolomite and micaceous sandstones grading to well-sorted white quartzites which are interbedded with grey to black shales of the Sullivan Shale Member.|
83943|Faugh-a-Balagh Member|70658|5|Briefly described|p7-8, 11, 21|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Peryhumuck Formation.||Is intruded by Lady Louise Suite.|Calc-albitite metasiltstone. Commonly ripple cross-bedded.|
34540|Finke beds""|22805|6|Mentioned|p471|Neoproterozoic|Neoproterozoic|||||||
34540|Finke beds""|23287|6|Mentioned|p102|||||||||
34540|Finke beds""|23288|6|Mentioned|p142 Fig.18|||Of Amadeus Basin.||||||18-SEP-06
34540|Finke beds""|64797|5|Briefly described|p155 Tb.1, p156, p161-163, p175|||S-isotope data.||||||
34540|Finke beds""|65365|5|Briefly described|p1, 5, 7, 10|Cryogenian|Cryogenian|Amadeus Basin. Unconformably overlain by Areyonga Formation.||||||
34540|Finke beds""|67326|5|Briefly described|p8|Neoproterozoic|Neoproterozoic|Informal name. Central Amadeus Basin.||||Overlies Bitter Springs Formation. Is overlain by Areyonga Formation.||
34540|Finke beds""|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
34540|Finke beds""|71080|6|Mentioned|p31|||Now Wallara Formation.||||||
24980|Finniss Formation""|38290|6|Mentioned|p40|||A suggested name which the author states as being pre-empted.||||||
70562|Finniss River Sandstone""|61525|6|Mentioned|p42 Tb.3|||Building stone used in University of Adelaide Old Classics Wing, Prince of Wales Building. Informal name.||||||02-JUN-06
76153|Finniss River beds|66623|6|Mentioned|p231.|Permian|Permian|[See Finniss Sand]||||||
28553|Finniss Sand|38290|5|Briefly described|p62|||||||||
39188|Finniss formation|23768|6|Mentioned|p34|||Informal name - refers to Finniss Clay.||||||29-MAR-05
37076|Flinders Gneiss""|23719|6|Mentioned|p9|||Of Whitten 1966a,b. Geological Province: Gawler Craton.||||||12-MAR-08
80392|Flinders Range Sandstone-Quartzite Series""|71242|14|Not recorded|p9|||Of Segnit (1939). Generally Pound Quartzite (Coats, 1965).||||||
39210|Flinders Slate|23731|5|Briefly described|p27|||Of Tapley Hill Formation.||||||
38531|Forest Hill Formation|24176|6|Mentioned|p13|Adelaidean|Adelaidean|Misspelt - see Fortress Hill Formation (of the Yerelina Sub-Group/Umberatana Group).||||||
35346|Fortress Hill Siltstone|23176|6|Mentioned|p14|||||||||
26304|Fountain Spring Beds|22889|6|Mentioned|p31,32|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Former Parent Unit - River Wakefield Subgroup, see p33 for details.||||||12-MAR-14
26304|Fountain Spring Beds|23054|5|Briefly described|p11-2|||||||||
26304|Fountain Spring Beds|36733|2|Defined|p70|Adelaidean|Adelaidean|See also P39.||||||
26304|Fountain Spring Beds|37854|6|Mentioned|p14|||||||||
26304|Fountain Spring Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26304|Fountain Spring Beds|40294|6|Mentioned|Table 2|||||||||
26304|Fountain Spring Beds|41404|4|Described|p94|||Mention P78||||||
26304|Fountain Spring Beds|42222|6|Mentioned|p13|||||||||
26304|Fountain Spring Beds|42274|5|Briefly described|p450|||||||||
26304|Fountain Spring Beds|43052|5|Briefly described|p177,Table 6.2|||of Emeroo Subgroup? or equivalent to?||||||12-MAR-14
26304|Fountain Spring Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
81770|Freeling Heights Conglomerate|67323|5|Briefly described|p36|||Mount Painter Inlier, northern Gawler Craton.|~1600-1590 Ma protolith deposition.|||||
29891|Freeling Heights Quartzite""|43052|6|Mentioned|p97|||||||||
82103|Freeling Heights quartzite|72459|6|Mentioned|p68, p98|||Adjacent to the British Empire Granite [though relationship not made clear].|||||Quartzite that is micaceous and feldspathic in part.|
81151|Fresh Well Formation, lower|70816|5|Briefly described|p5,17, 18|||Roopena-Myall Creek area, Gawler Ranges. See also Fresh Well Formation.||Unit of lower Gawler Range Volcanics.||Intruded by Angle Dam Volcanics.||
81151|Fresh Well Formation, lower|71129|4|Described|p69-70,73-74|Calymmian|Calymmian|Geological Province: Gawler Craton. Comprises one coarsening-upward package of volcaniclastic siliciclastic sediments. Thickness: 1-66m, to over 140m thick where peperite contacts occur in ROOPENA DDH1 and DDH 6. Has peperitic contacts with the Angle Dam Volcanics, and based on presence of both overlying and underlying relationships, is interpreted to have preceded Angle Dam Volcanic emplacement in the north, and post-dated ADV emplacement in the south. Depositional environments range from lacustrine in the north and fluvial to colluvial to the south; suggesting initial sedimentation within the lacustrine basin beign fed from the south and east (McAvaney and Wade, 2015b).||Unit of Gawler Range Volcanics.||Overlain by lower Roopena Basalt. Underlain by Angle Dam Volcanics.|Coarsening upwards cycles of dark grey finely laminated mudstones to laminated graded bedded siltstone with sandstone interbeds to fine-grained sandstones to lithic sandstone and polymict conglomerate.|
81151|Fresh Well Formation, lower|72237|4|Described|p28,30-32|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin. Marks the first phase of sedimentation in the Roopena Basin.||Unit of Gawler Range Volcanics.||Overlain by lower Roopena Basalt. Underlain by Angle Dam Dacite.|Alluvial conglomerates and sandstones.|
81151|Fresh Well Formation, lower|73162|4|Described|p452-454, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Deposition in alluvial fan to fluvial environment. Thickness ranges from less than 1 m to 14 m. Thickness of 140 m and 95 m in drill holes where the unit is brecciated, may not be indicative of depositional thickness.||Fresh Well Formation||Overlies the Angle Dam Dacite. Underlies the lower Roopena Basalt|Massive, poorly sorted polymict conglomerate, interlayered lithic sandstone, siltstone grading into conglomerate, pebble - cobble clasts in dolomitic quartzo-feldspathic matrix. Partially modified by tectonic-hydrothermal brecciation and alteration.|
81152|Fresh Well Formation, upper|70816|5|Briefly described|p5,17, 18|||Roopena-Myall Creek area, Gawler Ranges. See also Fresh Well Formation. SHRIMP U-Pb zircon geochronology of a tuff from upper FWF yielded crystallisation age of 1587+\-15 Ma (Johnson 1993).||Unit of lower Gawler Range Volcanics.||Interfingered with Roopena Basalt.||
81152|Fresh Well Formation, upper|71129|4|Described|p69-70,72-74,77|Calymmian|Calymmian|Geological Province: Gawler Craton. Comprises three coarsening-upward packages of volcaniclastic siliciclastic sediments, recording progradational packages of three rapid flooding events, potentially generated from extensional faulting (McAvaney and Wade, 2015b) . Thickness: 32-85m thick; indiviual coarsening-upwards cycles are 2-50m thick, typicall 15-30m, and tuffs at 0.5-6m thick. ||Unit of Gawler Range Volcanics.||Overlain by upper Roopena Basalt. Underlain by lower Roopena Basalt.|Coarsening upwards cycles of dark grey finely laminated mudstones to laminated graded bedded siltstone with sandstone interbeds to fine-grained sandstones to lithic sandstone and polymict conglomerate.|
81152|Fresh Well Formation, upper|72237|4|Described|p28,30-31|Mesoproterozoic|Mesoproterozoic|Geological province: Gawler Craton. Of Roopena Basin. Represents major phase of sedimentaion in the Roopena Basin, deposited in a fluviolacustrine setting. Characterised by three coarsening-upwards prograding sedimentary packages with sharp basal contacts, indicating rapid flooding events within the Roopena Basin with extra-basinal episodic explosive felsic volcanism during sedimentation. Dominated by magmatic zircons of the c. 1635-1605 Ma Saint Peter Suite (Curtis, Wade and Reid 2018); with a maximum depositioanl age of c. 1580 Ma.||Unit of Gawler Range Volcanics.||Overlain by upper Roopena Basalt. Underlain by lower Roopena Basalt.|Volcaniclastic claystone, siltstone and sandstone.|
81152|Fresh Well Formation, upper|73162|4|Described|p452-455, p458|Mesoproterozoic|Mesoproterozoic|Roopena Basin. Most extensive in southern part of basin, up to 84 m thick. Alluvial to lacustrine setting, contains slump folds. Detrital zircon signature shows input from the ca. 1635-1605 Ma St Peter Suite, and a minor component of Gawler Range Volcanic-aged zircon.||Fresh Well Formation|Whaler Hut Member, Stud Dam Member, Comet Bore Member.|Overlies the lower Roopena Basalt. Underlies the upper Roopena Basalt. Interlayered with the Whaler Hut, Stud Dam and Comet Bore members.|Coarsening-upwards packages of massive to finely laminated and dolomitic claystone, laminated siltstone, poorly to moderately sorted lithic sandstone, and massive clast supported conglomerate; rich in felsic volcanic detritus.|
37142|Fryers Formation|23565|5|Briefly described|p195|||Of Broken Hill Group||||||
68100|Fryers Metasediments|60485|5|Briefly described|p28 Fig. 2|||Of the Purnamoota Subgroup (Broken Hill Group).  Geological Province: Broken Hill Domain.||||||
68100|Fryers Metasediments|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Broken Hill Group.||||
68100|Fryers Metasediments|63102|5|Briefly described|p13|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Purnamoota Subgroup.||||
68100|Fryers Metasediments|70657|5|Briefly described|p13 Fig.6|Statherian|Statherian|Curnamona Province; Broken Hill Domain. See also Freyers Metasediments (p15).|<1693 Ma, >1650 Ma|Broken Hill Group||Underlies Sundown Group. Overlain by Hores Gneiss. Intruded by and overlies Parnell Gneiss.||
81670|Fullham Sand|70334|6|Mentioned|p69|||Of Adelaide Plains.||||||
81670|Fullham Sand|71129|6|Mentioned|p155|Pleistocene|Pleistocene|Of Adelaide Plains. Equivalent to Pleistocene aeolian sand sheets in SIX MILE HILL.||||||
76828|Gairdner Dykes|60515|5|Briefly described|p118|||Magnetite-bearing.|c. 800 Ma.||||Dolerite dykes.|
76828|Gairdner Dykes|65376|5|Briefly described|p12. |Neoproterozoic|Neoproterozoic|Formal name is Gairdner Dolerite. Related to earliest phases of rifting in the Adelaide Geosyncline.|827+/- 6 Ma.|||Interpreted as feeders to Beda Volcanics.||
76828|Gairdner Dykes|67030|5|Briefly described|p408|Cryogenian|Cryogenian|Accepted as feeder for the Beda Volcanics (Mason et al. 1978).|827 +/- 6 Ma (Wingate et al. 1998)|||Intrudes the Pandurra Formation (Schmidt & Williams 2011).||26-APR-12
76828|Gairdner Dykes|69003|6|Mentioned|p58|Proterozoic|Proterozoic|Mantle plume activity associated with the break-up of Rodinia.|c.825 Ma.|||||
76828|Gairdner Dykes|73155|5|Briefly described|p266, p284|Tonian|Tonian|Prevalent as NW-trending linear, high magnetic anomalies. Best recognised in Archean basement, south of the Skylark Fault Zone. Also shown as Gaidner Dyke p277-278.|ca. 830 Ma||||Variable gabbroic to doleritic composition.|
76828|Gairdner Dykes|74367|6|Mentioned|p7|||||||||
69475|Gairdner dolerite|61154|5|Briefly described|p5 Tb. 1, p32|Neoproterozoic|Neoproterozoic|Informal term used in the context of the Gairdner dolerite dykes in South Australia.  Age: 824+/-4Ma.  Geological province: Adelaide Fold Belt.||||||
69475|Gairdner dolerite|72725|6|Mentioned|p2|||[Written as Gairdner dolerite dykes.]||||||
69475|Gairdner dolerite|73184|6|Mentioned|p196|Tonian|Tonian|Intruded throughout the Musgrave Block and Gawler Craton. Potential source of Neoproterozoic detrital zircons in the Grant Group.|ca 825 Ma||||Dolerite dykes.|
78774|Gairdner dyke swarm|63562|6|Mentioned|p337|||Plume-related magmatism.|c. 800 Ma|||||06-DEC-17
78774|Gairdner dyke swarm|69437|5|Briefly described|p22:3, 12|||Of the Gairdner Large Igneous Province.  Intrudes Supersequence 1 in the Officer and Amadeus Basins.|c.825 Ma.|||Correlated with Amata Dolerite.||12-JUL-16
78774|Gairdner dyke swarm|69873|5|Briefly described|p73, p82|||Possible equivalent of Tayatea Dyke Swarm in Tasmania. Appears as Gairdner Dyke Swarm on p82. A similar age of 824 +/- 4 Ma is from Glikson et al., (1996).|827 +/- 6 Ma (Wingate et al., 1998).|||||
78774|Gairdner dyke swarm|70744|5|Briefly described|p939|||Magmatism was coeval with breakup of Rodinia (860-570 Ma).|827 Ma (Wingate et al., 1998).|||||
78774|Gairdner dyke swarm|72259|6|Mentioned|p1, p9|||[Written as Gairdner-Amata dyke swarm and Gairdner-Amata Dyke (G-A) dyke swarm].||||||
78774|Gairdner dyke swarm|72488|6|Mentioned|p16||||~825 Ma.|||||
78774|Gairdner dyke swarm|73166|6|Mentioned|p644|Neoproterozoic|Neoproterozoic|Gawler Craton. Intrudes the Olympic Cu-Au Province.|0.83 Ga|||||
69393|Gairdner suite|61153|6|Mentioned|p351|||Informal name. Geological Province: Amadeus Basin.||||||
82042|Gambier Limestone Member|72445|6|Mentioned|App.7 p7.|Oligocene|Oligocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991) as Gambier Limestone.||Said to be of  Murray Group||||
40219|Gambier Limestone, lower|24202|6|Mentioned|p321|||Informal reference to the Greenways Member of the Gambier Limestone.  Geological Province: Gambier Sub-basin.||||||
37085|Gap Well formation|23723|4|Described|p15|Proterozoic|Proterozoic|Overlying unit West Creek formation. Geological Province: Jillawarra basin. Max. thickness: 1400 m.||||||
24997|Garford Formation limestone|35080|6|Mentioned|p12|||||||||
76010|Gartners Calcarenite|50133|6|Mentioned|p7, p9 Tb.1|||Informal name for calcarenite from Gartners Quarry? Used as alternative name for Camelback Member. Geochemistry given.||||||
36995|Gawler Range Volcanics suite|23482|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Informal?||||||
36995|Gawler Range Volcanics suite|23731|6|Mentioned|p28|Mesoproterozoic|Mesoproterozoic|Informal - see Gawler Range Volcanics.||||||
38638|Gawler Range porphyry|24346|5|Briefly described|p99, p109|||Superseded by Yardea Dacite and Eucarro Rhyolite.||||||
68704|Gawler Range-Hiltaba volcano-plutonic complex|60704|6|Mentioned|p687, p697|Mesoproterozoic|Mesoproterozoic|Informal combination of Gawler Range Volcanics and Hiltaba Suite by Johnson and Cross (1995). Age: 1595-1575 Ma.||||||11-APR-05
41681|Gawler Ranges granite|50605|5|Briefly described|p8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite. Age: 1581 +/- 16Ma (U-Pb).||||||
41682|Gb suite|50605|5|Briefly described|p(ii), 1.3, 9.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary 1590 Ma Supersuite.||||||
35854|Gellibrand Member|23322|5|Briefly described|957 Fig.2|||Of the Gambier Limestone in South Australia.  Geological Province: Gambier Basin.  See also p968.||||||07-SEP-09
35854|Gellibrand Member|63124|5|Briefly described|p87 Fig. 5.29|Early Oligocene|Early Oligocene|Of Gambier Limestone but superseded by Gellibrand Marl of Heytesbury Group. Geological Province: Gambier Basin.||||||
67927|Geltwood Beach Formation""|44133|6|Mentioned|p144|||Superseded by Pretty Hill Formation.||||||
67927|Geltwood Beach Formation""|63124|6|Mentioned|p59|||Recommended this name be dropped from use. See also Geltwood Beach Formation. Originally used by Reynolds et al (1966) for a more lithic and shaly sandstone upper section of Pretty Hill Sandstone below Eumeralla Formation.||||||31-JAN-08
78430|Gerra Clay|65194|6|Mentioned|p26|||aquiclude||||||
23615|Gibbon Beds|23719|4|Described|p29|Pleistocene|Pliocene|See also page 27 Table 8. Overlain by Pooraka Formation. Underlain by Melton Limestone. Geological Province: Gawler Craton [???probably overlies]. Max. thickness: 90 m.||||||04-NOV-10
23615|Gibbon Beds|39349|6|Mentioned|Map legend||Pliocene|Pliocene to Pleistocene||||||
23615|Gibbon Beds|40448|5|Briefly described|p43|||||||||
23615|Gibbon Beds|43052|5|Briefly described|Table 2.1 p27|Pleistocene|Pliocene|Pirie Basin||||||
23615|Gibbon Beds|44133|5|Briefly described|p178|Pleistocene|Pliocene|Geological Province: Pirie Basin. Thickness: 10m. Overlies: Melton Limestone.||||||
23615|Gibbon Beds|67462|5|Briefly described|Map legend.|Pliocene|Late Miocene|Western Pirie Basin.||||||
23615|Gibbon Beds|70334|5|Briefly described|p60|||"Of Pirie Basin. [Misspelling of Gibbon beds]||||||22-NOV-19
68789|Gidgealpa Volcanics|24509|5|Briefly described|p42|Early Cambrian|Early Cambrian|Age: ~530-520Ma. Geological Province: Warburton Basin.||||||
68789|Gidgealpa Volcanics|66623|6|Mentioned|p431.|||Name changed to Gidgealpa Group. Cooper Basin. May represent a northerly extension of the Mount Wright Volcanic Arc in the Koonenberry Belt area.||||||
39864|Giles Complex intrusives|24497|6|Mentioned|Map legend|||Informal name - see Giles Complex.||||||
35684|Giles Mudstone|23282|6|Mentioned|p57|||of Sukanta (1993). Superced by Meramangye Formation.||||||
35684|Giles Mudstone|23287|6|Mentioned|Fig.2,4|||Age: Lower Ediacarian. of Eastern Officer Basin.||||||
35684|Giles Mudstone|23288|6|Mentioned|Fig.5,14|||||||||
26572|Giles ultrabasic intrusive complex|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran to Torrensian||||||
27416|Gillen Member|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Bitter Springs Formation. Dolomite, green siltstone, sandstone, shale, evaporites.  Geological Province: Amadeus Basin.||||||
27416|Gillen Member|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
27416|Gillen Member|22560|5|Briefly described|p4|||Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22561|4|Described|p16 & Fig 9|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22562|5|Briefly described|p34|||Averages 810m in thickness in the northern part of the Basin, p34. Of the Bitter Springs Formation.||||||06-FEB-08
27416|Gillen Member|22565|6|Mentioned|p71 in Table 1|||||||||
27416|Gillen Member|22566|4|Described|p74|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22646|5|Briefly described|p 99|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22647|5|Briefly described|p 113|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.  Overlying Unit - Loves Creek Member.||||||19-SEP-06
27416|Gillen Member|22649|6|Mentioned|p 140|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22651|6|Mentioned|Fig 11 btw p182-183|Proterozoic||||||||
27416|Gillen Member|22653|6|Mentioned|p 229||Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22762|5|Briefly described|p375|Neoproterozoic|Neoproterozoic|||||||
27416|Gillen Member|22763|6|Mentioned|p393|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22805|5|Briefly described|p472|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|22816|5|Briefly described|p10 Fig. 4|Neoproterozoic|Neoproterozoic|Bitter Springs Formation, Amadeus Basin||||||
27416|Gillen Member|22823|6|Mentioned|p514|Proterozoic|Proterozoic|Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|23282|6|Mentioned|p52|||May be equivalent to Alinya Formation.||||||
27416|Gillen Member|23286|5|Briefly described|p89||Neoproterozoic|Similar fossil assemblage to Alinya Formation. Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|23287|6|Mentioned|p102|||Of Bitter Springs Formation, Amadeus Basin. Holds major fossil assemblage of arcitachs.||||||19-SEP-06
27416|Gillen Member|23288|6|Mentioned|p142 Fig.18|||In the Amadeus Basin. Correlative of Alinya Formation due to acritarchs.||||||19-SEP-06
27416|Gillen Member|23314|5|Briefly described|331 Fig.2|||||||||
27416|Gillen Member|23361|5|Briefly described|16 Fig.4|Neoproterozoic|Neoproterozoic|Of Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|24301|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Of Bitter Springs Formation.  Geological Province: Amadeus Basin||||||06-FEB-08
27416|Gillen Member|32720|6|Mentioned|p7|||Bitter Springs Fm.||||||
27416|Gillen Member|32722|6|Mentioned|Fig.3|||Stromatolite. Adelaidean||||||
27416|Gillen Member|34488|6|Mentioned|p9|||Proterozoic. See also p10, Table 1.||||||19-SEP-06
27416|Gillen Member|34579|4|Described|Table 1|||See also p15.||||||19-SEP-06
27416|Gillen Member|34724|6|Mentioned|p342|||||||||
27416|Gillen Member|35102|6|Mentioned|p16|||||||||
27416|Gillen Member|35805|5|Briefly described|p36|||See also Fig.3.||||||
27416|Gillen Member|36751|6|Mentioned|p369|||||||||
27416|Gillen Member|38157|6|Mentioned|Table VI|||||||||
27416|Gillen Member|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27416|Gillen Member|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27416|Gillen Member|39210|4|Described|p29|||Stromatolites.||||||19-SEP-06
27416|Gillen Member|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27416|Gillen Member|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation. Limestone, sandstone, siltstone. Geological Province: Amadeus Basin.||||||14-FEB-06
27416|Gillen Member|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27416|Gillen Member|40740|3|Fully described|p9|||||||||
27416|Gillen Member|41190|6|Mentioned|Fig.4|||||||||
27416|Gillen Member|41203|6|Mentioned|p5|||||||||
27416|Gillen Member|41270|6|Mentioned|p276|||||||||
27416|Gillen Member|41509|6|Mentioned|p9|||||||||
27416|Gillen Member|41510|6|Mentioned|Map legend|Neoproterozoic||||||||
27416|Gillen Member|41618|5|Briefly described|p325|||||||||
27416|Gillen Member|41717|6|Mentioned|Fig.2|||||||||
27416|Gillen Member|41820|6|Mentioned|p17|||||||||
27416|Gillen Member|41852|6|Mentioned|Fig.2|||||||||
27416|Gillen Member|42082|6|Mentioned|Fig.3 P323|||||||||
27416|Gillen Member|42845|6|Mentioned|Fig.3 P498|||Of Bitter Springs Formation?||||||19-SEP-06
27416|Gillen Member|42886|5|Briefly described|Fig.2 P219|||Of the Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|42940|5|Briefly described|p1|||Of Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|43503|6|Mentioned|11-29|||Age from Ediacaran||||||19-SEP-06
27416|Gillen Member|43647|6|Mentioned|p530|||||||||
27416|Gillen Member|43756|6|Mentioned|p541|||||||||
27416|Gillen Member|44335|4|Described|p.7||Proterozoic|Table 1. p.8.||||||
27416|Gillen Member|44336|14|Not recorded|map legend||Proterozoic|SG/53-3. Of Bitter Springs Formation.||||||19-SEP-06
27416|Gillen Member|45041|4|Described|p24|||Proterozoic||||||
27416|Gillen Member|46730|5|Briefly described|p7|||Of Bitter Springs Formation. Overlying Unit: Loves Creek Member. Geological Province: Amadeus Basin||||||
27416|Gillen Member|48880|4|Described|p.15,Pl.11-13||Neoproterozoic|(F53-14,15,G53-3). U.Prot.||||||
27416|Gillen Member|48890|2|Defined|p.12||Neoproterozoic|See also Tables, Figs, Plates. pt. Bitter Springs Fm. U.Proterozoic.||||||
27416|Gillen Member|48963|6|Mentioned|Fig.2|||||||||
27416|Gillen Member|50246|5|Briefly described|p20 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation. Dolostone, limestone, shale, siltstone.||||||07-FEB-11
27416|Gillen Member|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Bitter Springs Formation. Geological Province: Amadeus Basin. Dolomite, green siltstone, sandstone, shale, evaporites.||||||
27416|Gillen Member|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Bitter Springs Formation.||||||
27416|Gillen Member|61309|5|Briefly described|p16 Fig. 4|||Of the Bitter Springs Formation. Geological Province: Amadeus Basin.||||||06-FEB-08
27416|Gillen Member|61732|5|Briefly described|p131|Cryogenian|Cryogenian|Of the Bitter Springs Formation. Contains Cryogenian assemblages (glacigenic successions, 850-600Ma).||||||07-FEB-11
27416|Gillen Member|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
27416|Gillen Member|62379|5|Briefly described|p7 Fig. 2, p34|Late Proterozoic|Late Proterozoic|Of the Bitter Springs Formation. Geological Province: Amadeus Basin.||||||
27416|Gillen Member|62453|5|Briefly described|p24|||Of the Bitter Springs Formation. Geological Province: Amadeus Basin||||||
27416|Gillen Member|62989|5|Briefly described|p40|||Of Bitter Springs Formation. Overlain by Loves Creek Member (Bitter Springs Formation). Geological Province: Amadeus Basin.||||||07-FEB-08
27416|Gillen Member|64625|5|Briefly described|p245 fig 2, p246, p250|||Amadeus Basin. Probably fed by the Gairdner Dyke Swarm. Locally folded and overturned.||Bitter Springs Formation.||Overlies Heavitree Quartzite. Overlain by Loves Creek Member.||
27416|Gillen Member|64778|6|Mentioned|p18, 21|Neoproterozoic|Neoproterozoic|Amadeus Basin. Thermal and maturation history modelling.||Bitter Springs Formation.||||
27416|Gillen Member|64793|6|Mentioned|p284 fig 3, p285 fig 4, p289, p293|Cryogenian|Cryogenian|||Bitter Springs Formation.||Overlies Heavitree Quartzite. Is overlain by Loves Creek Member.||
27416|Gillen Member|64794|6|Mentioned|p238 fig 2|Cryogenian|Cryogenian|The rank is not shown in Fig.2.||Bitter Springs Formation.||||
27416|Gillen Member|64796|5|Briefly described|p183-186, p192-193, p199-200, p204-205|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. 400m thick.||Bitter Springs Formation||Is overlain by Loves Creek Member.|Halite, gypsum, minor dolomite.|
27416|Gillen Member|64797|5|Briefly described|p154-156, p168 Tb.11, p155 Tb.1.|||See also p172 Tb.13. S-isotope data.||Unit in Bitter Springs Formation.||||
27416|Gillen Member|64809|5|Briefly described|p1-7, p14-24    |Late Proterozoic|Late Proterozoic|The main rock unit discussed in this article. Appears as Gillen member on p1 and Fig.2.||Of the Bitter Springs Formation.||Unconformably overlies (sheared contact) Heavitree Quartzite. Is overlain by Loves Creek Member.|Dolostone, siltstone, sandstone, evaporites.|
27416|Gillen Member|65233|3|Fully described|p3 Fig. 2, p4|Neoproterozoic|Neoproterozoic|Basal member of Bitter Springs Fm. Overlain by Loves Creek Mbr. Geol.prov: Amadeus Basin. Oil source rock potential in the thick transgressive black shale, overlain by stromatolitic dolostone, occasional grey shale and x-bedded sandstone; salt  succn.||||||07-FEB-11
27416|Gillen Member|65256|6|Mentioned|p9, p28|||Of Bitter Springs Formation. Contains spilites; correlatives of these spilites are dated at 790+/-40 Ma and 797+/-49 Ma. Said to be 820 Ma on p9.||||||
27416|Gillen Member|65365|5|Briefly described|p2, 5, p9 Fig. 3, p10 Fig. 4|Cryogenian|Cryogenian|Member of the Bitter Springs Formation. Underlies the Loves Creek Member.||||||19-MAR-12
27416|Gillen Member|65366|5|Briefly described|p23 Fig. 3|Cryogenian|Cryogenian|Member of the Bitter Springs Formation. Underlies the Loves Creek Member.||||||19-MAR-12
27416|Gillen Member|65410|5|Briefly described|p76.|||Contains clusters of coccoid cyanobacteria and mat-like fragments formed by benthic microbial communities; proportions of species vary considerably.||Unit in Bitter Springs Formation.|||Evaporite-rich.|
27416|Gillen Member|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|Amadeus Basin. Halite units up to 850m thick in wells; up to 2200m thick in seismic images.||Bitter Springs Formation.||Is overlain disconformably by Loves Creek Member.|Basal transgressive black shale overlain by stromatolitic dolostone, occasional grey shale and cross-bedded sandstone; an upper evaporite succession of thick halite between two dolostone/anhydrite units.|
27416|Gillen Member|67326|5|Briefly described|p2, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Bitter Springs Formation.||Overlies Dean and Heavitree Quartzites. Is overlain by Loves Creek Member.||
27416|Gillen Member|67479|5|Briefly described|p39|||||Basal member of the Bitter Springs Formation.||Overlain by the Loves Creek Member. Conformably underlain by the Heavitree Quartzite.||
27416|Gillen Member|67565|5|Briefly described|p38.|Neoproterozoic|Neoproterozoic|||Lower unit in Bitter Springs Formation.||Is overlain disconformably by Loves Creek Member.|Carbonate, evaporite and silt.|
27416|Gillen Member|68275|6|Mentioned|p55|||Amadeus Basin.||Bitter Springs Formation.|||Evaporites.|
27416|Gillen Member|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
27416|Gillen Member|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Amadeus Basin. Late Proterozoic age.||Of the Bitter Springs Formation.|||Siltstone, limestone, and dolomite.|
27416|Gillen Member|69003|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||Bitter Springs Formation.||Overlies Heavitree Quartzite. Is overlain by Loves Creek Member.||
27416|Gillen Member|69031|5|Briefly described|p4, p8, p21|||Amadeus Basin. The halite unit has caused considerable halotectonic deformation (complex fold patterns).||Basal Bitter Springs Formation.||Overlies Dean and Heavitree Quartzites. Is overlain disconformably by Loves Creek Member.|Contains a halite unit.|
27416|Gillen Member|69418|5|Briefly described|p3:36|||An extensive salt layer in this unit seals the Mount Kitty gas and helium prospect in the Heavitree Quartzite.||Bitter Springs Formation.||Overlies Heavitree Quartzite.|Includes salt layers.|12-JUL-16
27416|Gillen Member|69437|5|Briefly described|p22:15|Cryogenian|Cryogenian|Acts as a seal to the underlying Heavitree Quartzite.||Bitter Springs Formation.|||Includes an extensive salt layer.|12-JUL-16
27416|Gillen Member|69438|3|Fully described|p23:2,5,7-8,10-12,20,43,47,53-54,59-61|Cryogenian|Cryogenian|Wells et al. (1970). Amadeus Basin. Type section is S of Mount Gillen, just W of Alice Springs. Up to c.850m thick. Remobilised salt layers are recognised in seismic profiles. Strata are folded and/or dip steeply. Hosts the Undoolya Gap Cu prospect which has generally low metal values; also a minor unnamed iron ore occurrence. One of the most likely oil- and/or gas-prone units in the Basin. Forms a regional salt seal over Heavitree/Dean Quartzites reservoirs.||Bitter Springs Formation.||Paraconformably (gradationally) overlies Heavitree Quartzite. Is overlain by Loves Creek Member disconformably (locally unconformably).|Basal thick, transgressive black shale, overlain by dolostone, stromatolitic dolostone, grey shale and sandstone; then dolomite and anhydrite, overlain by thick halite, and another dolomite/anhydrite unit. Rare basalt/spilite layers.|12-JUL-16
27416|Gillen Member|69606|5|Briefly described|p2, p4 fig 2, p8, p18, p19|Cryogenian|Cryogenian|Amadeus Basin. Source rock for the Gillen petroleum system. Halite drives halotectonics in the basin and the salts forms the seal of the Gillen petroleum system. Outcrop is generally poor and patchy, covered by calcrete and sand.||Bitter Springs Formation||Overlies the Dean Quartzite and Heavitree Quartzite. Disconformably or unconformably overlain by the Loves Creek Member.|Dolostone, silicilcastic rocks and significant thicknesses of evaporites, most notably halite.|
27416|Gillen Member|69673|5|Briefly described|p63, p70, p73, p88, p90, p99, p104|Neoproterozoic|Neoproterozoic|Potential source rock. Unconventional gas potential.||Bitter Springs Formation||Overlies Dean Quartzite, conformably overlies Heavitree Quartzite, disconformably overlain by Loves Creek Member|Evaporites with halite.|
27416|Gillen Member|69937|5|Briefly described|v, vi, p3 Tb.1, p5-8, p37-38|Neoproterozoic|Neoproterozoic|Amadeus Basin. Likely zircon provenance discussed.|896 +/- 24 Ma (maximum depositional age).|Basal Bitter Springs Formation.||Paraconformably overlies Heavitree Quartzite.|Dolomite, green siltstone, micaceous quartz sandstone, shale and evaporites.|
27416|Gillen Member|70018|4|Described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the northern Amadeus Basin. Correlable to Pinyanna Beds in the southern Amadeus Basin. ||Unit of Bitter Springs Formation.||Lowermost unit of Bitter Springs Formation. Overlain unconformably by Loves Creek Member.|Dolomite, shale, halite and gypsum.|
27416|Gillen Member|70416|5|Briefly described|p65 Fig.2, p80|Cryogenian|Cryogenian|Amadeus Basin.||Bitter Springs Formation.||||
27416|Gillen Member|71841|6|Mentioned|iii,p1|||Of Amadeus Basin. See Gillen Formation. Superseded; upgraded to Formation status, formalised by Normington et al (2015), Normington and Donnellan (in review).||||||
27416|Gillen Member|71842|5|Briefly described|p2|Cryogenian|Cryogenian|Of Amadeus Basin. Nomenclature after Haines and Allen 2010 (Western Amadeus, WA), Edgoose 2013 (NE Amedeus, NT). Nomenclature now obsolete (status has been upgraded to Formation; See NTGS2017-005 and references therein).||Unit of Bitter Springs Formation.||Lowermost unit of Bitter Springs Formation. Overlain by Loves Creek Member. Underlain by Dean or Heavitree quartzites.||
27416|Gillen Member|72249|4|Described|p327-334,342|Neoproterozoic|Neoproterozoic|Of Amadeus Basin; Centralian Superbasin. Thickness: 400m. Depositional environment: marine, intepreted based on Sr, Rb and S isotopes, and biomarkers. See p329-334 for detailed sedimentological and petrography description, and biostratigraphic and isotopic analysis of drill core and outcrop from this study. In outcrop (DUMP field section), comprises fine-grained carbonaceous material with columnar stromatolites, evaporites and bituminous dolomite. Microfossils and biomarkers are consistent with low-diversity microbial communities (cyanobacterial microfossils). Evaporitic facies interpreted to have formed in a barred basin with poor ciculation, cut off from the ocean by a stromatolite barrier reef. C and S isotopic analysis also indicate a marine depositional environment in an intracratonic setting.||Unit of Bitter Springs Formation.||Lower unit of Bitter Springs Formation. Overlain by Loves Creek Member. Underlain by Heavitree Quartzite.|Halite and gypsum and minor carbonate, thin sporadic basic volcanics.|
27416|Gillen Member|72601|6|Mentioned|p7|||Elevated to Gillen Formation included in the Bitter Springs Group.||||||
27416|Gillen Member|72711|6|Mentioned|p5 Fig.3.|Tonian|Tonian|Amadeus Basin. Gorjan et al 2000.|c. 840 Ma.||||Marine evaporites (sulphate).|
27416|Gillen Member|73085|6|Mentioned|p1|||Superseded by Gillen Formation.||||||
27416|Gillen Member|73086|6|Mentioned|piii, p5, p7, p14, p17-18, p25, p151|||Superseded [see Gillen Formation]. Was divided into five informal units.||||||
27416|Gillen Member|73088|6|Mentioned|p1|||Superseded; see Gillen Formation||||||
67928|Glanville Formation""|44133|6|Mentioned|p226|||||||||
75098|Glen Ewen Sandstone|64769|6|Mentioned|p27|Neoproterozoic|Neoproterozoic|In South Australia. Name for a dimension stone, probably not intended as a formal name.||||||16-APR-09
80466|Glen Osmond Arkosic Quartzite""|71529|14|Not recorded|p1 |||Replaced by Mitcham Quartzite?||||||
39212|Glen Osmond Bluestone|23731|5|Briefly described|p27|||Of Belair Subgroup Shale.  Commercial name for siltstone rock used for walling.||||||
39212|Glen Osmond Bluestone|61237|5|Briefly described|p36|||Informal name. The term 'bluestone' is used here to describe rock, generally siltstone, used mainly for walling in the building industry. Quarried from the Belair Subgroup shale.||||||16-AUG-05
26577|Glen Osmond Slate|22889|5|Briefly described|p35|Adelaidean|Adelaidean|Superseded by the Glen Osmond Slate Member as the unit has been down graded from formation to member status, see p 35 for details of the change.  The former correlation of the Glen Osmond Slate with the Mintaro Shale is no longer supported.||||||
26577|Glen Osmond Slate|23818|4|Described|p60|Adelaidean|Adelaidean|Underlying unit: Beaumont Dolomite. Max. thickness:~1500 ft. Correlated with the Saddleworth Formation.||||||
26577|Glen Osmond Slate|30782|6|Mentioned|Table 2|||||||||
26577|Glen Osmond Slate|30801|6|Mentioned|p5|||Table P5-6||||||
26577|Glen Osmond Slate|31923|6|Mentioned|p9|||||||||
26577|Glen Osmond Slate|32510|6|Mentioned|Table 1|||||||||
26577|Glen Osmond Slate|32724|6|Mentioned|Fig.1|||Correlation. Torrensian||||||
26577|Glen Osmond Slate|33423|4|Described|p13|||||||||
26577|Glen Osmond Slate|34308|6|Mentioned|p189|||||||||
26577|Glen Osmond Slate|34535|6|Mentioned|p60|||Torrensian||||||
26577|Glen Osmond Slate|37461|6|Mentioned|Table 5.I|||||||||
26577|Glen Osmond Slate|38157|6|Mentioned|Table III|||||||||
26577|Glen Osmond Slate|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26577|Glen Osmond Slate|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
26577|Glen Osmond Slate|40442|5|Briefly described|Fig.4|||||||||
26577|Glen Osmond Slate|40852|6|Mentioned|Fig.3.2|||||||||
26577|Glen Osmond Slate|41404|5|Briefly described|p114|||||||||
26577|Glen Osmond Slate|42098|5|Briefly described|Table 2 P54|||||||||
26577|Glen Osmond Slate|42222|5|Briefly described|p15|||||||||
26577|Glen Osmond Slate|42733|6|Mentioned|map legend|Adelaidean||||||||
26577|Glen Osmond Slate|43052|5|Briefly described|p181,Table 6.1|||of Burra Group||||||
26577|Glen Osmond Slate|71237|14|Not recorded|p9|||||||||
75090|Glenaire Clay|64993|5|Briefly described|p24|Early Oligocene|Early Oligocene|Geological province: Otway Basin. Preserves an original aragonitic molluscan fauna (Darragh 1985).||||||
68722|Glenforslan formation|24558|6|Mentioned|p664, p666|Miocene|Miocene|Informal - see Glenforslan Formation.||||||08-SEP-20
72890|Glenroth Granite|63067|5|Briefly described|p2 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ~2500Ma. Gneissic granite, adamellite, granodiorite.||||||07-NOV-08
73761|Glensforlan Formation|63460|4|Described|p839 Fig. 2b, p840, 842,844-846|Early Miocene|Early Miocene|Of the Morgan Group. Overlies Finniss Formation; underlies Cadell Fm. Thickness: 40m. Geological province: Murray Basin. Calcarenite and calcisiltite interbedded with marl in outcrop; base is foraminiferal limestone. Shown [correctly] as Glenforslan Formation p847.||||||08-SEP-20
73761|Glensforlan Formation|72445|6|Mentioned|App.6 p2 Fig.1.|Middle Miocene|Middle Miocene|Of Gallagher and Gourlay (2007), Lukasik and James (1998). [misspelling of Glenforslan]||Murray Supergroup||Overlies Finniss Formation and underlies Cadell Formation.|Includes limestone.|
29882|Gneiss Complex|24590|5|Briefly described|p44 Fig. 2.5|Archean|Archean|Not a formal name - but referred to as part of Mount Edgar Complex in which the Moolyella Adamellite Suite occurs. Same as Central Gneiss Complex? See also p40. Fig. 2.3, p55, p107.||||||07-FEB-11
29882|Gneiss Complex|31320|6|Mentioned|p.8||Precambrian|||||||
29882|Gneiss Complex|43052|6|Mentioned|p51|||refers to Miles (1954)||||||
42509|Gneiss Complex""|23818|6|Mentioned|p32|||||||||
42509|Gneiss Complex""|61556|6|Mentioned|p8|||Underlie the Middleback Group.||||||21-NOV-07
29881|Gneiss Group|43052|6|Mentioned|p51|||refers to Johns (1961)||||||
42485|Gneiss"" Complex|23818|5|Briefly described|p27 Fig.6, p30|Precambrian|Precambrian|Of the Cleve Metamorphics. Max. thickness:>15000 ft. Age: 2800-1600 Ma. Geological Province: Gawler Block.||||||
82104|Golden Pole granite|72459|4|Described|p64-65, p73, p86-89, p94-99|Mesoproterozoic|Mesoproterozoic|Together with the Wattleowie granite, Terrapinna Granite, White Well Granite and the Petermorra Volcanics forms sub""group"" 2b of this report. Geochemically identical to the Con Bore granite and therefore the authors suggest they are the same unit on opposite ends of a fold; in light of this the authors suggest use of Con Bore granite be discontinued and replaced with Golden Pole granite. Outcrops to north western margin of the Mount Painter Inlier on opposite limbs of the Mt Freeling syncline. Geochemistry indicates this unit is more fractionated than the Terrapinna and Wattleowie granites.||Moolawatana Suite|||Red, equigranular granite, fine to coarse-grained, often highly altered.|
29461|Gordon Limestone (SA)|34287|6|Mentioned|p71|||See also P84.||||||
29461|Gordon Limestone (SA)|42966|5|Briefly described|p407|||synonym of Pata Limestone||||||
69759|Gosse Pile pyroxenite intrusion|44109|4|Described|p10, p46|Mesoproterozoic|Mesoproterozoic|Informal part Giles Complex mafic-ultramafic intrusions. Near-vertically dipping sequence of pyroxenite-dominated cumulates, separated by a major fault from the Mount Davies intrusion. Max. thickness: >2000m.||||||
69759|Gosse Pile pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: >2000m.||||||
36098|Granite at Minnipa, Wudinna and Buckleboo 36098|43052|5|Briefly described|Table 5.6 p129|Mesoproterozoic|Mesoproterozoic|Unnamed units. Pinkish, coarse-grained granite-adamellite, minor porphyritic varieties and minor aplite dykes.||||||
23637|Greenfield Formation|24261|5|Briefly described|p1057|Calymmian|Statherian|Post 1984 the'volcanic member' of  Greenfield Formation was reinterpreted as volcanic diatremes. SHRIMP Age: 1597 +/- 8Ma therefore minimum age for Greenfield Formation [which now appears to be included in the Olympic Dam Breccia Complex]. Geological Province: Gawler Craton||||||21-SEP-18
23637|Greenfield Formation|39047|3|Fully described|p807|||||||||
23637|Greenfield Formation|41125|6|Mentioned|p31|||See also Fig.18||||||
23637|Greenfield Formation|41493|5|Briefly described|Table 2|||||||||
23637|Greenfield Formation|42022|6|Mentioned|p5|||||||||
23637|Greenfield Formation|42162|6|Mentioned|p57|||||||||
23637|Greenfield Formation|42169|5|Briefly described|p122|||See also Fig.3||||||
25030|Greenfield Formation Volcanic Member|41891|6|Mentioned|p304|||||||||
75061|Grindstone Range Formation|64829|6|Mentioned|p1083||Late Cambrian|May be misspelt?  See also Grindstone Range Sandstone. Geological province: Arrowie Basin.||||||07-FEB-11
75061|Grindstone Range Formation|65892|6|Mentioned|p9 Fig.4, p11. |Middle Cambrian|Middle Cambrian|[Name superseded]. See also Grindstone Range Sandstone (p7 Fig.3).||||||
75061|Grindstone Range Formation|68735|6|Mentioned|p235 Fig.3|Middle Cambrian|Middle Cambrian|Arrowie Basin. See also Grindstone Range Sandstone (p233 Fig.2, p235-236, p238).||||||10-APR-17
75061|Grindstone Range Formation|68993|5|Briefly described|p543, p544 Fig.1|Middle Cambrian|Middle Cambrian|This name is used as often as not instead of the current name, Grindstone Range Sandstone, even within the same paragraph.||||||
67929|Grindstone Range Sandstone, upper|44133|6|Mentioned|p30|||Informal name. See Grindstone Range Sandstone.||||||
31928|Grindstone Range sandstone|43876|14|Not recorded|p549||Middle Cambrian|||||||
76054|Gubberamunda Siltstone|65119|6|Mentioned|p512 Fig.6|||See Gubberamunda Sandstone p504 etc.||||||07-MAR-12
29471|Gum Creek Formation|42966|6|Mentioned|p179|||Of Ludbrook 1959, 1963.||||||
29471|Gum Creek Formation|73596|6|Mentioned|p1165|Neoarchean|Neoarchean|Youanmi Terrane. Shallow-marine to subaerial conditions.|c.2730 Ma.|||||
81628|Gunson beds''|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Woomera area.Of Adelaide Geosyncline.||||Overlain by Woocalla Dolomite Member. Undelain by McLeay beds. Transitional to Tapley Hill Formation.||16-SEP-19
27792|Hallett Arkose|22510|6|Mentioned|p40|||Name abandoned. Junior synonym of Marino Arkose.  Not related to Pliocene Hallet Cove Sandstone.||||||13-OCT-04
27792|Hallett Arkose|30378|6|Mentioned|p431|||||||||
27792|Hallett Arkose|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27792|Hallett Arkose|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|Marinoan||||||
27792|Hallett Arkose|40442|5|Briefly described|Fig.4|||||||||
27792|Hallett Arkose|41405|4|Described|p184|||||||||
77496|Hammerhead Delta supersequence|61230|5|Briefly described|p318.|Maastrichtian|Turonian|Thick succession of marine deltaic, shelfal to upper bathyal sediments that developed in the early Great Australian Bight.||||||
75625|Hampton Formation (Eucla)|23989|5|Briefly described|p54 Fig. 46|Late Eocene|Early Eocene|Misspelt in figure. See Hampton Sandstone.||||||
38730|Hampton Sandstone, upper|24397|5|Briefly described|p234 Tb. 2|||As used in NE margin of Eucla Basin. Replaced by Khasta Formation.  Geological Province: Eucla Basin.||||||19-FEB-15
38729|Hampton sandstone, upper|24397|6|Mentioned|p244|||Informal - see Hampton Sandstone.  Geological Province: Eucla Basin.||||||
42414|Hanging Knoll Intrusive|60662|6|Mentioned|Map Legend|||Of Giles Complex.||||||22-FEB-05
39180|Harlequin Stone""|24475|6|Mentioned|p57|||Informal name of Conor (1996).||||||
40178|Harris Greenstones|24597|6|Mentioned|p532 Fig. 5, p533|Archean|Archean|Probably an informal name - referring to rocks of the Harris Greenstone Belt.  Geological Province: Gawler Craton.||||||07-NOV-08
67930|Hawker Group, upper|44133|6|Mentioned|p28|||Informal name. See Hawker Group.||||||
67931|Heatherdale Shale, lower|44133|5|Briefly described|p10|||Informal, see Heatherdale Shale.||||||
72811|Heatherdale Shale, upper|23981|6|Mentioned|p8-9 Fig. 4, p10 Fig. 5, p26|Early Cambrian|Early Cambrian|Informal - see Heatherdale Shale.  Age: 526+/-4Ma (U-Pb SHRIMP: Copper et al, 1992).||||||04-FEB-08
68691|Heatherdale Shales|9124|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Kanmantoo Group. Mottled and nodular carbonaceous shales with phosphate nodule bands, locally calcareous at base.||||||11-JAN-10
68691|Heatherdale Shales|23981|6|Mentioned|p12|||Superseded by Heatherdale Shale.||||||
74003|Heatherdale Tuff|61307|5|Briefly described|p14 Fig. 6|Early Cambrian|Early Cambrian|Part of Heatherdale Shale unit? Age: 526+/-4Ma. ||||||
74003|Heatherdale Tuff|71139|6|Mentioned|p156|||Presented as Heatherdale tuff.||||||
39669|Heysen Supergroup, lower|24175|6|Mentioned|p12|Neoproterozoic|Neoproterozoic|Informal name for Umberatana Group, the lowermost part of the Heysen Supergroup (not covered in this study).||||||
39671|Heysen Supergroup, upper|24175|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Informal name for Wilpena Group, the uppermost part of the Heysen Supergroup (not covered in this study).||||||
75994|Heyson Supergroup|65376|6|Mentioned|p9 Fig.1.2. |Neoproterozoic|Neoproterozoic|Mis-spelling of Heysen Supergroup.||||||
75994|Heyson Supergroup|65379|6|Mentioned|p643|||Includes Umberatana Group.||||||07-MAR-12
73547|Heytsbury Group|12781|6|Mentioned|p386|Miocene|Eocene|Otway Basin.|||Compton Conglomerate; Gellibrand Marl, Gambier Limestone.|Unconformably overlies Nirranda Group.||
73547|Heytsbury Group|63124|4|Described|p91|||Probably misspelt - see Heytesbury Group. ||||||
39598|Hideaway Bore Member|40431|6|Mentioned|p13|||Misspelling of Hideaway Well Member.||||||
25056|Hideaway Creek Member|40431|6|Mentioned|p16|||Misspelling of Hideaway Well Member.||||||
82105|Hiltaba Granite Supersuite|72459|5|Briefly described|p10|Mesoproterozoic|Mesoproterozoic|Terminology of Creaser (1989).||||||
30135|Hiltaba Granite suite|43094|4|Described|p32|||||||||
37802|Hiltaba Granites|24169|5|Briefly described|p672|||||||||
37802|Hiltaba Granites|60657|5|Briefly described|p13 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Geological Province: Gawler Craton.||||||10-MAY-05
76836|Hiltaba Granitoid Suite|67027|6|Mentioned|p351 Table 1.|||See Hiltaba Suite.||||||
31373|Hiltaba Intrusive Complex|43561|6|Mentioned|Fig 3,p1434|||Variation on Hiltaba Granite?||||||
81671|Hiltaba Subsuite|70334|6|Mentioned|p90|||Geological province: Gawler Craton. [Cultana Subsuite of Hiltaba Suite?]||||||21-NOV-19
39233|Hiltaba Suite Calca Granite|23908|5|Briefly described|p6|Mesoproterozoic|Mesoproterozoic|Age: ~1456Ma. Probably an informal name. Geological Province: Gawler Craton.||||||
30412|Hiltaba Suite Granite|22851|6|Mentioned|13|Mesoproterozoic|Mesoproterozoic|||||||
30412|Hiltaba Suite Granite|43141|6|Mentioned|Fig.1 p63|||Informal use?||||||
30412|Hiltaba Suite Granite|43634|6|Mentioned|p12-13|||||||||
30412|Hiltaba Suite Granite|43635|6|Mentioned|p14|||||||||
30412|Hiltaba Suite Granite|63067|5|Briefly described|p2 Fig. 1|Mesoproterozoic|Mesoproterozoic|Age: ~1590Ma. Granite, adamellite, granodiorite, syenite, quartz monzodiorite.||||||
83526|Hiltaba Suite Volcanics|73516|6|Mentioned|p2|Calymmian|Calymmian|Gawler Craton. [Misspelling?] See also Hiltaba granites p6.|1595-1575 Ma|||||
35061|Hiltaba Suite granites|22515|6|Mentioned|p405,407|||||||||
35061|Hiltaba Suite granites|24217|6|Mentioned|p833|||Formal name not intended.||||||
35061|Hiltaba Suite granites|24261|5|Briefly described|p1048|Mesoproterozoic|Mesoproterozoic|Hiltaba Suite granites also referred to as the Hiltaba Supersuite granitoids. Geological Province: Gawler Craton||||||
35061|Hiltaba Suite granites|24365|6|Mentioned|p8|||Informal - see Hiltaba Suite.||||||
35061|Hiltaba Suite granites|24505|6|Mentioned|p6, p8|Mesoproterozoic|Mesoproterozoic|Informal - refers to granites of the Hiltaba Suite. Geological Province: Gawler Craton.||||||15-SEP-05
35061|Hiltaba Suite granites|24597|6|Mentioned|p529, p531|||Informal - see Hiltaba Suite.  See also p537.  Geological Province: Gawler Craton.||||||
35061|Hiltaba Suite granites|60484|6|Mentioned|p41|||Informal - see Hiltaba Suite.||||||
35061|Hiltaba Suite granites|60716|6|Mentioned|p10, p11|||Informal name.||||||
40177|Hiltaba Suite granitoid|24597|6|Mentioned|p529|||Informal - see Hiltaba Suite.   Granitoid of high magnetic intensity (Koondoolka Pluton).  Geological Province: Gawler Craton.||||||
40177|Hiltaba Suite granitoid|62729|5|Briefly described|p39 Fig. 1b|Mesoproterozoic|Mesoproterozoic|Age: 1595-1570 Ma. Informal name. See also Hiltaba Suite granitoids. Geological Province: Gawler Craton.||||||
38535|Hiltaba Suite granitoids|23805|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Formal name not intended - see Hiltaba Suite.  Intrude the Palaeoproterozoic Hutchison Group and Lincoln Complex granitoids.  Geological Province: Gawler Craton.||||||
38535|Hiltaba Suite granitoids|24261|5|Briefly described|p1048|Mesoproterozoic|Mesoproterozoic|Hiltaba Suite granitoids also referred to as the Hiltaba Supersuite granitoids. Geological Province: Gawler Craton||||||
38535|Hiltaba Suite granitoids|24346|6|Mentioned|p106 Fig.5|||Informal name - see Hiltaba Suite.||||||
38535|Hiltaba Suite granitoids|24475|6|Mentioned|p46|||Informal - see Hiltaba Suite.||||||
38535|Hiltaba Suite granitoids|24511|6|Mentioned|p58|||Informal.||||||
38535|Hiltaba Suite granitoids|50127|6|Mentioned|p50|||Informal name.||||||27-MAY-04
38535|Hiltaba Suite granitoids|60484|6|Mentioned|p41|||Informal - see Hiltaba Suite.||||||
38535|Hiltaba Suite granitoids|60716|6|Mentioned|p10|||Informal name. Geological Province: Gawler Craton.||||||
38535|Hiltaba Suite granitoids|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
38535|Hiltaba Suite granitoids|62727|5|Briefly described|p9|Mesoproterozoic|Paleoproterozoic|Informal name - refers to granitic rocks of the Hiltaba Suite. Uranium-enriched rocks.  Geological Province: Gawler Craton.||||||07-NOV-08
38535|Hiltaba Suite granitoids|62729|5|Briefly described|p40|Mesoproterozoic|Mesoproterozoic|Informal name. See also Hiltaba Suite granitoid. Geological Province: Gawler Craton.||||||
68785|Hiltaba Suite intrusive|24507|6|Mentioned|p25|||Informal. Referring to granite of Hiltaba Suite.||||||
37081|Hiltaba Suite""|23719|6|Mentioned|p17|||||||||
39920|Hiltaba Supersuite granitoids|24261|5|Briefly described|p1047 Fig.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton||||||
25058|Hiltaba granite|24197|6|Mentioned|p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name - see Hiltaba Granite. Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
25058|Hiltaba granite|36507|6|Mentioned|p116|||||||||
25058|Hiltaba granite|40241|6|Mentioned|p115|||||||||
25058|Hiltaba granite|60515|6|Mentioned|p120||||c. 1588 Ma.|||||
25058|Hiltaba granite|62978|6|Mentioned|p166 Fig. 3|Mesoproterozoic|Mesoproterozoic|Informal name for Hiltaba Granite. Geological Province: Gawler Craton.||||||07-FEB-11
37773|Hiltaba granite suite|24168|5|Briefly described|p634|||Informal name.||||||
83527|Hiltaba granites|73516|6|Mentioned|p6|||A-type. [Mistaken as part of Ninnerie Supersuite?]||||||
74606|Hiltaba magmatic suite|64233|6|Mentioned|p22|||Informal name. In the Gawler Craton.||||||18-SEP-08
83032|Hiltaba suite|73061|6|Mentioned|p1067|Mesoproterozoic|Mesoproterozoic|A-type granites. [Hiltaba Suite?]|||||Granites.|
83032|Hiltaba suite|74367|6|Mentioned|p4, p23|Calymmian|Calymmian||ca. 1590 Ma|||||
69745|Hinckley Range Gabbronorite|61340|5|Briefly described|Map legend|||Presented as the compound name Hinckley Range Gabbronorite/Troctolite Intrusion.||||||21-SEP-05
69746|Hinckley Range Troctolite|61340|5|Briefly described|Map legend|||Presented as the compound name Hinckley Range Gabbronorite/Troctolite Intrusion.||||||
72712|Hindmarsh Clay""|62898|6|Mentioned|p198|||Of Firmin (1967a, 1967b). Overlies Precambrian granites.||||||
83033|Hot Spring Gneiss|73061|6|Mentioned|p1076 Fig.6|Calymmian|Calymmian|Mount Painter Province. Diagram illustrates metamorphic ages in the 1540-1560 Ma range, and other ages (interp not clear) around 1580 Ma, apparently from this study, but not discussed further.||||||
34032|Houghton Diorite|22603|6|Mentioned|p96|Cryogenian|Tonian|850 Ma||||||
29896|Houghton calcsilicate""|43052|5|Briefly described|p103|||||||||
69734|Hutchinson Group metasediments|24505|6|Mentioned|p10|||Informal and misspelt - see Hutchison Group.  Geological Province: Gawler Craton. Hosts gold mineralisation.||||||24-JAN-06
37075|Hutchinson Group""|23719|5|Briefly described|p9|||Of Johns (1961). Geological Province: Gawler Craton.||||||27-FEB-08
38346|Hutchinson Group, Upper|23791|6|Mentioned|p4|||Informal - see Hutchinson Group.  Geological Province: Gawler Craton.||||||
37077|Hutchinson Schist""|23719|6|Mentioned|p9|||Of Whitten 1966a,b. Geological Province: Gawler Craton.||||||24-JUN-09
82106|Hutchinson group|72459|6|Mentioned|p21, p51|||Misspelling of the Hutchison Group.||||||
69793|Hutchison "Metamorphics"|61556|5|Briefly described|p8|||Contains iron formations. Overlies Flinders "Gneiss".||||||
25953|Hutchison Group|22489|5|Briefly described|p12|Orosirian|Orosirian|||||||
25953|Hutchison Group|22613|6|Mentioned|p10|||||||||
25953|Hutchison Group|22629|4|Described|fig2p147, 148, 149|Orosirian|Orosirian|Thickness: 3500m.||||||27-FEB-08
25953|Hutchison Group|22690|6|Mentioned|P305|Orosirian|Orosirian|Age of unit is 1991+/-7 to 1845+/-9 Ma||||||
25953|Hutchison Group|22834|6|Mentioned|P39||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|22854|6|Mentioned|P9||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|22910|6|Mentioned|40|||||||||
25953|Hutchison Group|22920|6|Mentioned|44|||||||||
25953|Hutchison Group|23124|5|Briefly described|p397|||||||||
25953|Hutchison Group|23285|4|Described|p 335|||||||||
25953|Hutchison Group|23491|6|Mentioned|p18||Paleoproterozoic|Of Donington Granitoid Suite.   Age:>/-1860Ma||||||07-NOV-08
25953|Hutchison Group|23492|6|Mentioned|p6||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|23719|4|Described|p12|Paleoproterozoic|Paleoproterozoic|Overlain by Myola Volcanics.  Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|23805|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Intruded by Hiltaba Suite granitoids.  Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|24261|5|Briefly described|p1047 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: >1600Ma. Geological Province: Gawler Craton||||||07-NOV-08
25953|Hutchison Group|24365|6|Mentioned|p4, p5 Fig.2|||||||||26-NOV-04
25953|Hutchison Group|24422|6|Mentioned|p84 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|24505|5|Briefly described|p5 Fig.1|||See also the misspelt and informal Hutchinson Group metasediments.  Geological Province: Gawler Craton.||||||24-JAN-06
25953|Hutchison Group|24526|5|Briefly described|P98, p97 Fig. 3|Paleoproterozoic|Paleoproterozoic|Multiple units of quartzite, schist, dolomite and iron formations.  Unconformably overlies the Mitalie Gneiss (place name is Miltalie).  Age: ~1800Ma.  Geological Province: Gawler Craton.  See also p96 Fig. 2, p98 Fig. 4.||||||07-NOV-08
25953|Hutchison Group|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Intruded by the Lincoln Complex.  Geological Province: Gawler Craton.  See also p525.||||||07-NOV-08
25953|Hutchison Group|30256|6|Mentioned|p287|||Refers Johns(1961)||||||
25953|Hutchison Group|31034|4|Described|p129|||Also mention Fig. 2||||||
25953|Hutchison Group|31320|6|Mentioned|p13|||In Cleve Metamorphics||||||
25953|Hutchison Group|32030|6|Mentioned|p190|||Precambrian||||||
25953|Hutchison Group|33466|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
25953|Hutchison Group|33727|6|Mentioned|p35|||Refers John (1961)||||||
25953|Hutchison Group|34615|6|Mentioned|p5|||||||||
25953|Hutchison Group|34834|6|Mentioned|p213|||||||||
25953|Hutchison Group|35021|6|Mentioned|p157|||||||||
25953|Hutchison Group|35078|6|Mentioned|p257|||||||||
25953|Hutchison Group|36507|5|Briefly described|p116|||||||||
25953|Hutchison Group|36627|6|Mentioned|p81|||||||||
25953|Hutchison Group|37461|6|Mentioned|Fig.5.2|||||||||
25953|Hutchison Group|37620|6|Mentioned|p7|||||||||
25953|Hutchison Group|37621|6|Mentioned|p14|||||||||
25953|Hutchison Group|37811|2|Defined|p229|Paleoproterozoic|Paleoproterozoic|See also Fig.2||||||07-NOV-08
25953|Hutchison Group|38068|5|Briefly described|p66|||||||||
25953|Hutchison Group|38969|6|Mentioned|p218|||||||||
25953|Hutchison Group|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|39844|6|Mentioned|p60|||||||||
25953|Hutchison Group|40003|5|Briefly described|Table 3|||||||||
25953|Hutchison Group|40227|6|Mentioned|p44|||||||||
25953|Hutchison Group|40430|6|Mentioned|Table 2|||||||||
25953|Hutchison Group|40445|5|Briefly described|p49|||||||||
25953|Hutchison Group|40448|4|Described|p30|||||||||
25953|Hutchison Group|40644|4|Described|p120 Fig. 2, p124 Fig. 3, p128-9|Mesoproterozoic|Paleoproterozoic|Includes the sub-unit Middleback Subgroup. Geological province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|41239|6|Mentioned|p94|||||||||
25953|Hutchison Group|41325|6|Mentioned|p15|||||||||
25953|Hutchison Group|41327|6|Mentioned|p3|||||||||
25953|Hutchison Group|41402|6|Mentioned|p35|||||||||
25953|Hutchison Group|41493|6|Mentioned|Table 1|||||||||
25953|Hutchison Group|41501|5|Briefly described|p88|||||||||
25953|Hutchison Group|41526|6|Mentioned|p14|||||||||
25953|Hutchison Group|41609|6|Mentioned|Fig.1|||||||||
25953|Hutchison Group|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
25953|Hutchison Group|41667|5|Briefly described|p5|||||||||
25953|Hutchison Group|41682|6|Mentioned|p14|||||||||
25953|Hutchison Group|41972|5|Briefly described|p365|||||||||
25953|Hutchison Group|41973|6|Mentioned|p387|||||||||
25953|Hutchison Group|42167|6|Mentioned|Fig.4P117|||||||||
25953|Hutchison Group|42468|5|Briefly described|Fig.1 P2|||||||||
25953|Hutchison Group|42469|5|Briefly described|p10|||Palaeoproterozoic||||||
25953|Hutchison Group|42546|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25953|Hutchison Group|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25953|Hutchison Group|42738|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25953|Hutchison Group|42934|5|Briefly described|p520 Fig.1|||||||||
25953|Hutchison Group|43048|5|Briefly described|p10|||||||||
25953|Hutchison Group|43049|6|Mentioned|p28|||||||||
25953|Hutchison Group|43052|4|Described|p54|||see also Fig.4.2||||||
25953|Hutchison Group|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Schist, iron formation, calcsilicate, marble, amphibolite. Includes Bosanquet Formation. Geological Province:Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|43094|6|Mentioned|p42|||||||||
25953|Hutchison Group|43141|6|Mentioned|p63,Fig.1||Proterozoic|||||||
25953|Hutchison Group|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|43561|6|Mentioned|p1438|||||||||
25953|Hutchison Group|43583|6|Mentioned|p2163|||||||||
25953|Hutchison Group|43595|4|Described|p354||Paleoproterozoic|||||||07-NOV-08
25953|Hutchison Group|44935|5|Briefly described|Map Legend||Proterozoic|||||||
25953|Hutchison Group|50605|6|Mentioned|p2.1|||Geological Province: Gawler Craton & Curnamona Province. Intruded by: Donington Granitoid Suite, Minbrie Gneiss, Younger Lincoln Suite.||||||
25953|Hutchison Group|60534|5|Briefly described|p571-572, Fig.1, p587|Paleoproterozoic|Paleoproterozoic|Metasediments. Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartzitic, pelitic and calcsilicate metasediments, iron formation, marble, amphibolite.||||||07-NOV-08
25953|Hutchison Group|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated metasediments and metavolcanics. Geological Province: Gawler Craton.||||||23-JUL-13
25953|Hutchison Group|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Quartzitic, pelitic schist and calcsilicate metasediment, iron formation, marble and amphibolite.||||||07-NOV-08
25953|Hutchison Group|61307|5|Briefly described|p36 Fig. 17, p37|Paleoproterozoic|Paleoproterozoic|Age: ~1964-1850Ma; a separate interpretation puts the age at 1810Ma, about 150-50My younger than the ages published by Fanning et al (1988) and Rankin et al (1988). Thickness (est.): ~5000m. Geol Prov: Gawler Craton.||||||23-JUL-13
25953|Hutchison Group|61393|5|Briefly described|p169.|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks. Separated from the Donington Suite granites by the Kalinjala Shear Zone.|1900 - 1850 Ma.|||||23-SEP-14
25953|Hutchison Group|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
25953|Hutchison Group|61659|6|Mentioned|p30 Fig.1. |Paleoproterozoic|Paleoproterozoic||||||Paragneisses.|
25953|Hutchison Group|61725|5|Briefly described|p887|Paleoproterozoic|Paleoproterozoic|Overlies the Sleaford Complex. Geological Province: Gawler Craton. See also Hutchison Group metasediments, a term used more in this study than the formal nomenclature for the group.||||||
25953|Hutchison Group|62729|5|Briefly described|p39 Fig. 1b, p40|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks; BIF. Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|62893|4|Described|Map Legend, p10, p12-15, p25, 28, p36-38|Early Proterozoic|Early Proterozoic|Probably includes the Bosanquet Formation. Represents a sequence of fluvial to marine clastic and chemical sediments plus minor mafic volcanics. Deformation occurred during the Kimban Orogeny (1850 Ma to 1650 Ma) and resulted in interleaving with the Sleaford Complex. Hosts minor base metal mineralisation.|||Yadnarie Schist, Middleback Subgroup, Middleback Jaspilite (Upper and Lower), Cook Gap Schist, Katunga Dolomite, Warrow Quartzite|Unconformably overlain by Blue Range Beds. Intruded by Lincoln Complex.|Metamorphosed mixed clastic and chemical sedimentary rocks including dolomitic marble, banded calc-silicate gneiss, minor ferruginous cherty quartzite, and schist.|
25953|Hutchison Group|63020|5|Briefly described|p987|Paleoproterozoic|Paleoproterozoic|Age: >1718Ma. Intruded by Moody Suite and Middlecamp Granite. Geological Province: Gawler Craton.||||||07-NOV-08
25953|Hutchison Group|63275|6|Mentioned|p13, p14 Fig.1, p16.|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula.||||||
25953|Hutchison Group|63398|5|Briefly described|p663|Paleoproterozoic|Paleoproterozoic|Age: 2000-1860Ma.||||||07-NOV-08
25953|Hutchison Group|63866|4|Described|p5, p9, p19-p21, p30|Orosirian|Orosirian|Coulta, Spencer and Cleve Domains, Gawler Craton. Radically different interpretations as to the age of this group has been proposed in which it is suggested that the Hutchison Group is younger than the Donington Suite [and thus the latter would not intrude the former].|c. 2000-1860 Ma (unit relationships)||Includes the Warrow Quartzite, Bosanquet Formation and the Middleback Subgroup.|Unconformably overlies the Miltalie Gneiss, Wangary Gneiss, Hall Bay Volcanics and the Dutton Suite. Intruded by the Donington Suite.|Overall fining upwards sequence of sedimentary rocks.|
25953|Hutchison Group|64130|5|Briefly described|p1378-1380 Fig.2, p1382, p1836 Fig.5 |Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton. Variably deformed and metamorphosed.|c.2000-1857 Ma||Includes Middleback Subgroup and Bosanquet Formation.|Unconformably overlies the Miltalie Gneiss.|Basal sequence of quartzite and massive dolomite; overlain by carbonates, interlayered pelitic units and iron-formations; upper part consists of pelitic rock types and felsic volcanics and volcaniclastics.|
25953|Hutchison Group|64131|5|Briefly described|p1399-1402, p1404-1409       |Paleoproterozoic|Paleoproterozoic|Post-Sleafordian orogeny. Shallow- to deep-water sequence with interbedded volcanic rocks. Intrusion by Donington Granitoid Suite c. 1.85 Ga. Petrophysical properties.|<2000-1850 Ma|||Is intruded by Donington Granitoid Suite.|Believed to consist of quartzites and banded iron formation (BIF), with minor calc-silicates,metapelites, and amphibolites.|
25953|Hutchison Group|64133|5|Briefly described|p1443, p1464 Fig.15 |Paleoproterozoic|Paleoproterozoic|Deposited on a passive margin to the E of Archean core.|Between ~2000 Ma and ~1845 Ma (Hand et al., 2007)|||||
25953|Hutchison Group|64137|5|Briefly described|p1542 Fig.1, p1543,   |Paleoproterozoic|Paleoproterozoic|Hosts the Wilcherry Hill gold prospects.||||||03-MAR-15
25953|Hutchison Group|64313|5|Briefly described|p450, p457|Paleoproterozoic|Paleoproterozoic|Contains the Bosanquet Formation. Age: ca.1850Ma or younger. Geological province: Gawler Craton. See also Fig. 1.||||||09-FEB-10
25953|Hutchison Group|64576|6|Mentioned|p625 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: c. 1960-1860Ma.||||||
25953|Hutchison Group|64722|4|Described|p12-13|Statherian|Neoarchean|See also mis-spelt Hutchinson Group. A mixed clastic and chemical sedimentary succession containing 2720-2000 Ma detrital zircons. Upper part contains 1850 and 1790 Ma detrital zircons.||||Unconformably overlies Sleaford Complex and Miltalie Gneiss.||11-APR-12
25953|Hutchison Group|64739|6|Mentioned|p264 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
25953|Hutchison Group|64828|5|Briefly described|p1065 Fig. 2|Paleoproterozoic|Paleoproterozoic|Unconformably overlies the Sleaford Complex units.||||||04-MAR-09
25953|Hutchison Group|65221|5|Briefly described|p26, 27, p28 Fig.3, p29 Fig.4, p32|Palaeoproterozoic|Palaeoproterozoic|Chemical and clastic sediments. Stratigraphic position, age and constituent units under review. Intruded by Gawler Range Volcanics and Hiltaba Suite. Includes Bosanquet Formation, Warrow Quartzite, Katunga Dolomite and Middleback Subgroup.||||||14-MAR-10
25953|Hutchison Group|65375|4|Described|p7, pp12-13, pp43-44.|Paleoproterozoic|Paleoproterozoic|Growth of the Gawler Craton proceeded eastwards by accreting this and other Groups to the Archean core. Sediments thought to have been deposited in a primeval rift basin.|1920-1860 Ma.||Includes Bosanquet Formation.|Unconformably overlies Miltalie Gneiss.|High-grade metamorphic siliciclastics and carbonates.|
25953|Hutchison Group|65376|4|Described|p11, pp54-64, p142.|Paleoproterozoic|Paleoproterozoic|Shallow-marine sediments; underwent high-grade metamorphism, partial melting and complex deformation from 1730-1700 Kimban Orogeny. Subsequently intruded by porphyritic rhyolite dykes with synchronous mineralisation.|Deposited between 2000 Ma and 1850 Ma.||Includes basal Warrow Quartzite, Middleback Subgroup, Yadnarie Schist and Bosanquet Formation.|Overlies Dutton Suite and Carnot Gneiss.|Clastic and chemical metasediments, including iron-formation.|
25953|Hutchison Group|65379|5|Briefly described|p641, p643, 651|Paleoproterozoic|Paleoproterozoic|Includes Middleback Subgroup and Warrow Quartzite. Metasedimentary and metavolcanic rocks, unconformably overlies Archean basement. N.B. Asbestos deposit host.||||||07-MAR-12
25953|Hutchison Group|65390|5|Briefly described|p17, p19, p23 Fig.3|Statherian|Orosirian|Cleve Domain, Gawler Craton. Also spelt Hutchinson Group / Hutchinson Group metasediments, in text. Shallow clastic and chemical marine sediments, with minor acid and mafic volcanics. Includes (Parker and Lemon, 1982) Warrow Quartzite, Middleback Subgroup, Yadnarie Schist. Unconformably overlies Miltalie Gneiss. Intruded by Moody Suite. Hosts Pb-Zn mineralisation including the Menninnie Dam prospect.||||||
25953|Hutchison Group|65483|6|Mentioned|p17 Fig. 1|Palaeoproterozoic|Palaeoproterozoic|||||||
25953|Hutchison Group|65485|5|Briefly described|p42, Fig 1|Orosirian|Orosirian|Shallow to deep marine chemical and clastic sediments.|2000-1860 Ma.|||Overlies the Sleaford Complex.|Includes quartzite, dolomite, banded iron formation and pelitic to psammitic schist.|19-MAR-12
25953|Hutchison Group|65772|6|Mentioned|p229 Fig.2|Orosirian|Orosirian|c.1960-1860 Ma.||||||
25953|Hutchison Group|65915|4|Described|p2, p3 Fig.2, p5, p18|Orosirian|Orosirian|Overlies Sleaford Complex and Miltalie Gneiss. Correlated with Middleback Subgroup, but correlation now questioned. Clastic and chemical sedimentary rocks. Interpreted depositional setting is a shallow continental shelf in a passive margin. <2000-1850? Ma.||||||
25953|Hutchison Group|65922|4|Described|p9, p12-15, p29 Fig. 6, p30, p36-37|Orosirian|Orosirian|Overlies Archean basement, Gawler Craton. Consists of basal quartzite (Warrow Quartzite) overlain by marble, calcsilicate, cherty BIF and schist (Middleback Subgroup). Has metamorphic age of ~1845-1700 Ma. Sedimentation age constrained to <1950 - 1845 Ma by U-Pb zircon ages of the stratigraphically lower Miltalie Gneiss. Metamorphosed and deformed during Kimban Orogeny, with syntectonic granite intrusions.||||||
25953|Hutchison Group|66302|4|Described|p4 Fig.3, p6, p18-19, p24, p33-34, p57|Paleoproterozoic|Paleoproterozoic|Coulta, Spencer and Cleve Domains, Eastern Gawler Craton. Deposited on a passive margin, continental shelf environment between 2000-1860 Ma. See also p62, p64, p65 Fig.16, p76 Fig.20, p77 Fig.21, p87. |||Includes the Warrow Quartzite, Katunga Dolomite, Lower Middleback Jaspilite,  Burrawing Amphibolite, Cook Gap Schist, Upper Middleback Jaspilite, Yadnarie Schist and the Bosanquet Formation.|Overlies the Sleaford Complex. Intruded by the Donington Suite.|Metasedimentary rocks, extrusive mafic and felsic volcanic rocks.|
25953|Hutchison Group|66882|4|Described|p99-104, p107, p109-112, p121|Statherian|Neoarchean|Southern to central-northern South Australia Craton. Previously assigned as one stratigraphy, now superseded and broken into three Groups; Middleback Group, Darke Peak Group and Cleve Group. Underwent amphibolite to granulite facies metamorphism; potential geochemistry effects discussed.|Age 2500-1730 Ma.||Included Yadnarie Schist and Bosanquet Formation.|||03-MAR-15
25953|Hutchison Group|66916|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Eyre Peninsula.|c.1860-1790 Ma.|||||
25953|Hutchison Group|67027|6|Mentioned|p348.|||||||Is overlain unconformably by Blue Range Beds.||
25953|Hutchison Group|67058|5|Briefly described|p476.|Paleoproterozoic|Paleoproterozoic|Shallow marine sequences.|>1866 +/- 10 Ma (Fanning et al. 2007).|||Overlies Miltalie Gneiss.||
25953|Hutchison Group|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 1960 - 1860 Ma|||||
25953|Hutchison Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||See also p32 Fig.4.4. Gawler Craton.|~1760-1740 Ma.||Warrow Quartzite, Bosanquet Formation.|||
25953|Hutchison Group|67536|6|Mentioned|Map Legend|||Gawler Craton.|||||Quartzitic, pelitic and calcsilicate metasediments.|
25953|Hutchison Group|67721|5|Briefly described|p32|Orosirian|Orosirian|Extends from the southern Eyre Peninsula to the Olympic Dam region. Geochronology by Parker and Lemon (1982); Parker (1993)|2000-1865 Ma||Includes the Middleback Group?|||
25953|Hutchison Group|67900|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|Eastern Gawler Craton. Previously included rocks now assigned to the Darke Peak Group.||||||
25953|Hutchison Group|67980|6|Mentioned|p550|Paleoproterozoic|Paleoproterozoic|||||||
25953|Hutchison Group|68021|6|Mentioned|p139|||Gawler Craton.||||||
25953|Hutchison Group|68131|5|Briefly described|p2 Fig.1, p58, p61|Paleoproterozoic|Paleoproterozoic|Parker (1978, 1980) and Parker and Lemon (1982). Eastern Eyre Peninsula. Relative age of this unit and the Donington Suite is discussed in some detail.|||Warrow Quartzite, Middleback Subgroup, Yadnarie Schist.||Clastic and chemical metasediments, including iron formation.|
25953|Hutchison Group|68158|5|Briefly described|p4-5, p17|Paleoproterozoic|Paleoproterozoic|W of the Kalinjala Shear Zone. Parts of this unit are included in the Lincoln Complex. The stratigraphically highest subgroup is the 1800-1780 Ma Cleve Succession.|1850-1790 Ma.||Warrow Quartzite, Katunga Dolomite, Lower Middleback Jaspilite, Middleback Subgroup.||Schist and amphibolite.|
25953|Hutchison Group|68208|6|Mentioned|p32 Fig.3, p33, p34 Fig.5, p35|Paleoproterozoic|Paleoproterozoic|Cooyerdoo Granite most likely is basement to the Hutchison Group in the Middleback Range.  Hutchison Group in the Middleback Range may be an older package (Neoarchean) that is distinct from the Paleoproterozoic Hutchison Group  rocks occuring elsewhere in the Gawler Craton, based on the work of Szpunar et al. 2011.  Shows strong fabric from Kimban Orogeny.||||Probably overlies Cooyerdoo Granite.||
25953|Hutchison Group|69048|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|Southern Eyre Peninsula.||||||
25953|Hutchison Group|69554|6|Mentioned|p130|Paleoproterozoic|Paleoproterozoic|Szpunar et al. (2011). Gawler Craton.|||||Volcano-sedimentary sequence.|
25953|Hutchison Group|69591|6|Mentioned|p105 Fig.2.99, p106 Fig.2.100|||Appears (as Upper Hutchison Group ?) in diagrams of the geodynamic setting of ~1870-1820 (Fig.2.99) and~1760-1740 Ma (Fig.100) Ma eastern Australia.||||||
25953|Hutchison Group|69649|6|Mentioned|p6 Fig.4||||||||Includes paragneisses.|
25953|Hutchison Group|69666|6|Mentioned|p27 Fig.3|Paleoproterozoic|Paleoproterozoic|||||||
25953|Hutchison Group|70027|5|Briefly described|p56,58|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Metasedimentary assemblage intruded by Moody Suite monzonitic and leucogranitic rocks.||||||
25953|Hutchison Group|70405|6|Mentioned|p12 figure 4|Paleoproterozoic|Paleoproterozoic||1800 Ma|||||
25953|Hutchison Group|70511|6|Mentioned|p86|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||Surrounds (?is intruded by) Roxby Downs Granite.||
25953|Hutchison Group|70721|6|Mentioned|p63-p64|Paleoproterozoic|Paleoproterozoic||||||Ironstones.|
25953|Hutchison Group|70816|5|Briefly described|p4|Paleoproterozoic||Gawler Ranges region. Outcrops in the Middleback Range.||||Underlain by Cooyerdoo Granite.|Includes iron formations.|30-MAY-19
25953|Hutchison Group|70948|5|Briefly described|p975|Paleoproterozoic|Archean|Geological province: Gawler Craton.||||Underlain by Cooyerdoo Granite basement.|Includes iron formations.|
25953|Hutchison Group|71037|5|Briefly described|p20-21, p21 Fig.1, p24|Paleoproterozoic|Paleoproterozoic|Developed as part of a large, lithologically complex shallow marine basin that includes the Wallaroo Group.||||Shown as younger than Bosanquet Formation and older than Myola Volcanics and Broadview Schist.||
25953|Hutchison Group|71129|6|Mentioned|p14,p17-18,203|Statherian|Orosirian|Geological Province: Cleve-Coulta Domain, Gawler Craton.|2000-1790 Ma||Includes the Middleback Subgroup.|Contemporaneous with Myola Volcanics and Broadview Schist.||13-NOV-19
25953|Hutchison Group|71235|5|Briefly described|p1, p3-p4, p6, p8-p9, p14|Palaeoproterozoic|Palaeoproterozoic|Deformed and metamorphosed to upper greenschist-amphibolite grade during the Kimban Orogeny.|2000-1850 Ma||Includes the Middleback Subgroup and Katunga Dolomite.|Unconformably overlain by the Corunna Conglomerate and Blue Range Beds.||16-MAR-23
25953|Hutchison Group|71236|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|||||||
25953|Hutchison Group|71317|5|Briefly described|p15-p16|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.|1790 Ma|||||
25953|Hutchison Group|71322|6|Mentioned|p104, p108, p119, p135|||Replaced in part by Cleve Group (Szpunar et al., 2011).||||||
25953|Hutchison Group|71341|6|Mentioned|p188 fig 7, p194|||||||||
25953|Hutchison Group|71348|6|Mentioned|p201,211,216|Statherian|Statherian|Geological province: Gawler Craton.||||||
25953|Hutchison Group|71413|5|Briefly described|p32, 37|Orosirian|Orosirian|Geological province: Gawler Craton. Described as undifferentiated Hutchison Group on p32.|1964-1850 Ma|||Intruded by Samphire granite?|Includes metasedimentary rocks.|
25953|Hutchison Group|71418|5|Briefly described|p20,24|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Regional metasedimentary rocks that host epithermal alteration at Nankivel Hill, Eyre Peninsula. Alteration data c. 1585 Ma based on dating of alunite within the advanced argillic alteration assemblage. 40Ar/39Ar dating of allunite from siliceous breccia include ages of 1586+\-8 and c. 1590  Ma, interpreted to be hydrothermal crystallisation ages (Acidic alteration age: Benduzu et al., 2008).|||Includes Katunga Dolomite.|||
25953|Hutchison Group|71534|6|Mentioned|p296|Statherian|Statherian|Geological province: Gawler Craton.||||||
25953|Hutchison Group|71536|6|Mentioned|pp21, p80, p83, p94, p96||||||Includes the Wilgerup schist.|||
25953|Hutchison Group|71559|6|Mentioned|p15 Fig 1, p16 Fig 2|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton.||||||
25953|Hutchison Group|71859|5|Briefly described|p3-p4, p6, p11, p18, p35-p36|Paleoproterozoic|Paleoproterozoic|Cleve and Coulta domains, southern Gawler Craton.|c. 2000- 1790 Ma||Includes the Warrow Quartzite, Bosanquet Formation, Cook Gap Schist, Katunga Dolomite and the Upper and Lower Middleback Jaspilite.|||25-OCT-22
25953|Hutchison Group|71862|5|Briefly described|p2-p3, p6, p13, p15|Paleoproterozoic|Paleoproterozoic|See also  p17, p19, p44, p52-p53.|c. 1790 Ma|||Intruded by the Moola Suite and the Moody Suite including the Uranno Microgranite, Carappee Granite and the Chinmina Monzonite. Faulted against the Donington Suite.|Metasedimentary rocks.|
25953|Hutchison Group|72058|5|Briefly described|p172|||Cleve Domain, Gawler Craton. Excludes the Middleback Group succession in the Middleback Ranges area.|||||Chemical and clastic metasedimentary rocks including economically significant banded iron formations.|16-MAR-21
25953|Hutchison Group|72090|4|Described|p1, p8, p10, p13-p14, p17, p73|Statherian|Orosirian|Gawler Craton. Hosts a magnetite-rich magnesian skarn at the base which features a sub-economic Pb-Zn-Ag deposit. Three samples which potentially belong to this group are described. See also p78, p81, p86-p87, p101-p102, p111-p115, p119-p120.|c. 1865-1740 Ma||||Pegmatite, magnetite rich magnesian skarn and calc-silicate rocks.|
25953|Hutchison Group|72459|5|Briefly described|p8, p21|Mesoproterozoic|Mesoproterozoic|Occurs in the Cleve subdomain of the Gawler Craton where it overlies Archaean dominated basement. Misspelt as Hutchinson group on p21.|||||Sedimentary rocks.|
25953|Hutchison Group|72462|6|Mentioned|p3, p10|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Reflects a passive continental margin setting.||||Underlain by Sleaford Complex.||
25953|Hutchison Group|72463|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
25953|Hutchison Group|72464|5|Briefly described|p3, 10, 16, 20, 27|||Nankivel Dam area, Gawler Craton. Samples of alunite produced mimimum ages for alunite crystallisation of c.1590-1586 Ma.|||||Metasedimentary rocks including muscovite-bearing quartzite.|
25953|Hutchison Group|72484|5|Briefly described|p2||||~2.566 Ma (MDA: Szpunar et al., 2011).||Darke Peake, Cleve, Middleback Subgroups.|Overlies Cooyerdoo Granite.|Metamorphosed chemical and clastic sediments.|
25953|Hutchison Group|72488|6|Mentioned|p2 Fig.1|||Eastern Gawler Craton.|~1.96 Ga.|||||
25953|Hutchison Group|73026|5|Briefly described|p5, p7, p13, p25|Orosirian|Orosirian|Occurs structurally above the Miltalie Gneiss. Recent zircon studies suggest this unit is an amalgamation of units of differing provenance and potentially significantly different maximum depositional ages (Szpunar et al, 2011). This unit was thus seperated into the Darke Peak Group and the Cleve Group.|c. 1850 Ma|||||
25953|Hutchison Group|73027|5|Briefly described|p5, p7, p13|Palaeoproterozoic|Palaeoproterozoic||c. 1850 Ma|||||
25953|Hutchison Group|73030|6|Mentioned|p2148-2149|Statherian|Orosirian|Gawler Craton.||||||
25953|Hutchison Group|73092|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
25953|Hutchison Group|73103|5|Briefly described|Map legend.|||Is shown in the Solid Geology Interpretation map, below the main Whyalla 250k map.||||||
25953|Hutchison Group|73104|6|Mentioned|p2-4, p15, p72|||Inferred basement rock of the Mount Double area.|c. 2000-1730 Ma||||Includes metasediments. May include pegmatite, magnetite-rich magnesian skarn and calc-silicate.|
25953|Hutchison Group|73107|5|Briefly described|Map legend.|||||||Possible equivalent to Corny Point Paragneiss protolith.||
25953|Hutchison Group|73110|5|Briefly described|Map legend.|||Shown in the Solid Geology Interpretation map below the main PORT AUGUSTA map.||||||
25953|Hutchison Group|73130|6|Mentioned|[poster]|Statherian|Statherian|Constitutes basement beneath the Itiledoo Basin.|c. 1790 Ma|||||
25953|Hutchison Group|73155|5|Briefly described|p264 Fig.1, p265, p279-281|Statherian|Orosian|Gawler Craton, southern. Correlated with Mount Woods Metamorphics and Skylark Metasediments. May be preserved within the Mount Woods Inlier. See also Hutchison Group equivalents p282-283.|ca. 2000-1740 Ma, ca. 1860 Ma||Darke Peak Group||Metasedimentary rocks including meta-arkose, metasiltstone, metapelite and psammopelite.|
25953|Hutchison Group|73235|5|Briefly described|p53, p57-59, p61, p63|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Cleve and Coulta regions. Hosts gold mineralisation in the Southern Gawler Range Volcanics mineral field of the Kararan (Gawler Range Volcanics) gold mineral system. Hosts Tank Hill and Weednanna epithermal gold mineralisation. Deposited in a shallow marine, shelf environment. Exact composition is still uncertain; geochronology has suggested a wide age distribution of very similar packages of stratigraphy which had previously been interpreted as correlatives.|||||Mainly consists of clastic and chemical sediments including banded iron formations, carbonates, and gneiss.|
25953|Hutchison Group|73493|5|Briefly described|p712, p716 Fig.3|||Gawler Craton, south.|||||Shale, siltstone or schist, conglomerate, mafic volcanics, sandstone, dolomite, iron formation.|
25953|Hutchison Group|74361|6|Mentioned|p163|Paleoproterozoic|Paleoproterozoic|Gawler Craton. Deformed by the Kimban Orogeny (1730-1690 Ma).|2000-1866 Ma.|||||
78887|Hutchison Group Metasediments|62641|6|Mentioned|p277 Fig.1. |Paleoproterozoic|Paleoproterozoic|Gawler Craton.|2.0-1.85 Ga.|||||20-MAY-14
83523|Hutchison Group equivalents|73155|6|Mentioned|p282 Fig.13, p283|Orosian|Orosian|Oldest sedimentary package recognised in the Mount Woods Domain.|ca. 1860 Ma|Mount Woods Metamorphics||||
68955|Hutchison Group metasediments|24508|5|Briefly described|p30|||Consists of quartzite, dolomite, BIF, mafic volcanics and pelite. Geological Province: Gawler Craton.||||||23-DEC-09
68955|Hutchison Group metasediments|61070|6|Mentioned|Map Legend|||||||||12-JAN-10
68955|Hutchison Group metasediments|61725|5|Briefly described|p887|Paleoproterozoic|Paleoproterozoic|Informal reference to metasediments within the Hutchison Group. Overlies the Sleaford Complex.||||||
68955|Hutchison Group metasediments|62727|6|Mentioned|p11|Paleoproterozoic|Paleoproterozoic|Informal name - refers to sediments of the Hutchinson Group (which probably should be Hutchison Group?). Geological Province: Gawler Craton.||||||07-NOV-08
69463|Hutchison Group paragneiss|24526|5|Briefly described|p97 Fig. 3|||Informal reference to paragneiss within the Hutchison Group. Age of depsoition: ?2000-1700Ma. Geological Province: Gawler Craton.||||||
29825|Hutchison Metamorphics|43052|6|Mentioned|p51|||refers to Whitten (1966).||||||
37122|Ice Brook formation|23562|5|Briefly described|p294|||Informal.||||||
34336|Ifould Complex|22629|6|Mentioned|fig2p147|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
34336|Ifould Complex|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
34336|Ifould Complex|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34336|Ifould Complex|24422|5|Briefly described|p84 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1740-1670 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
34336|Ifould Complex|24522|6|Mentioned|p82|Paleoproterozoic|Paleoproterozoic|Age: 1.65-1.55Ga (Daly et al 1998; Fitzsimons 2002). ||||||07-NOV-08
34336|Ifould Complex|24526|5|Briefly described|p97 Fig. 3, p100|Mesoproterozoic|Paleoproterozoic|Synorogenic granitoid plutons named by Daly et al (1998).  Age: 1620-1550Ma.  Geological Province: Gawler Craton.  See also p96 Fig. 2.||||||07-NOV-08
34336|Ifould Complex|24583|6|Mentioned|p12|||Geological Province: Gawler Craton.||||||06-MAY-05
34336|Ifould Complex|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1740-1670Ma.  Geological Province: Gawler Craton.  See also p530.||||||07-NOV-08
34336|Ifould Complex|60484|6|Mentioned|p32|||Of Teasdale (1997). Name now abandoned.||||||03-MAR-05
34336|Ifould Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Age: ~1650-1540Ma. Orogenic intrusives. Of the Kararan Orogeny.||||||07-NOV-08
34336|Ifould Complex|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Variably deformed I-type gabbro to granite, Kararan Orogeny. Age: ~1680-1540 Ma.||||||07-NOV-08
34336|Ifould Complex|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1750Ma. Geological Province: eastern Gawler Craton.||||||07-NOV-08
34336|Ifould Complex|62641|6|Mentioned|p287 Fig.10(b).||||c.1.73-1.6 Ga.|||||
34336|Ifould Complex|62978|6|Mentioned|p???|||Informal name for Ifould Suite? Geological Province: Gawler Craton.||||||07-FEB-11
34336|Ifould Complex|64131|6|Mentioned|p1404|Paleoproterozoic|Archean||||||Mid-lower crustal meta-intrusions.|
34336|Ifould Complex|64725|6|Mentioned|p58 Fig.2.|||Gawler Craton.||||||
34336|Ifould Complex|64726|6|Mentioned|p83 Fig.2.|Paleoproterozoic|Paleoproterozoic|Western Gawler Craton. Episodic arc-type magmatism. Interpreted as relics of a continental arc emplaced in response to north-dipping subduction.|c.1740-1670 Ma.|||||
34336|Ifould Complex|65376|6|Mentioned|p10, p125.|||This term has been abandoned.|||Includes Tunkillia and St Peter Suites and Nuyts Volcanics.|||
34336|Ifould Complex|65390|5|Briefly described|p21, p24|Statherian|Statherian|Name used by Teasdale (1997) for variably-deformed I-type granitoids and mafics at Lake Ifould, western Gawler Craton. Daly et al. (1998) used the name for all syntectonic Kararan Orogeny intrusives. This article proposes Teasdale's usage as having precedence, and proposes the stratigraphic term Ifould Suite. Age of 1672 +/- 17 Ma.||||||
34336|Ifould Complex|65922|4|Described|p9, p14 Tb.1, p16, p29 Fig. 6|Statherian|Statherian|Of Teasdale (1997). Includes Symons and Carappee Granites. Medium to coarse-grained foliated granite with xenoliths of foliated banded gneiss; isoclinally folded with sheared limbs. 1670 +/-17 Ma (U-Pb zircon).||||||
34336|Ifould Complex|69648|4|Described|p12 Fig.6, p13, p15-16, p33, map legend|Mesoproterozoic|Paleoproterozoic|Intrudes felsic metasediments of Mulgathing Complex. Christie Subdomain, western Gawler Craton. Daly et al. (1998) defined these intrusive rocks as Ifould Complex from "Fowler Suture Zone" (now Fowler Domain). ||||Intrudes Mulgathing Complex; considered as correlatives of part of the Tunkillia Suite (Ferris and Schwarz, 2004).|Intermediate to felsic intrusives; co-magmatic granite-diorite complexes, include granodiorite gneiss (Rb-Sr age 1667 +/- 115 Ma), migmatitic quartz-feldspar-biotite gneiss (Rb-Sr 1703 +/- 1106 Ma), gneissic granite, aplite and pegmatite.|
34336|Ifould Complex|69649|5|Briefly described|p36|Paleoproterozoic|Paleoproterozoic|Teasdale (1997); subsequently included in Tunkillia Suite by Ferris (2005). Daly et al. (1998) used Ifould Complex for all syntectonic Kararan Orogeny intrusives.|||||Variably-deformed I-type granitoids and mafics.|
30618|Ifould Lake granite gneiss|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Informal name. Age: 1750-1700Ma.||||||07-FEB-11
30618|Ifould Lake granite gneiss|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1667 +/- 115Ma (Rb-Sr). Of the Younger Lincoln Supersuite.||||||07-NOV-08
68084|Ifould Suite|60484|6|Mentioned|p32|||Of Daly et al  (1998)?  Name now abandoned.||||||
68084|Ifould Suite|61659|5|Briefly described|p30 Fig.1, p33, p37, p39.   |Paleoproterozoic|Paleoproterozoic|Associated with magmatic arc processes. S.G. = 2.84 +/- 0.04. Correlated with the Muckanippie Anorthosite Complex.|1690 - 1670 Ma (Teasdale 1997).|||Intrudes Christie Domain.|Felsic to mafic plutons.|
68084|Ifould Suite|62978|5|Briefly described|p161, p164, p180|Mesoproterozoic||Ages: ~1680Ma, and 1670Ma. Intrudes the Christie Gneiss. Geological Province: Gawler Craton.||||||07-FEB-11
68084|Ifould Suite|63866|6|Mentioned|p31|||||||||
68084|Ifould Suite|64722|6|Mentioned|p14|Statherian|Statherian|Also referred to as Lake Ifould Suite. A product of extensive granite magmatism in the Gawler Province that occurred mainly between 1690-1670 Ma.||||||11-APR-12
68084|Ifould Suite|64726|6|Mentioned|p82, p88.|||See Ifould Complex.||||||
68084|Ifould Suite|65390|5|Briefly described|p21, p24|||New term proposed for I-type granitoids and mafics near Lake Ifould, western Gawler Craton, described by Teasdale (1997) as 'Ifould Complex'. It is unclear if age of 1672 +/- 17 Ma given here for granites in Lake Ifould area is for the'Ifould Suite'.||||||
68084|Ifould Suite|65487|6|Mentioned|p61|||Emplaced 1740-1640 Ma in the western Gawler Craton. Interpreted 'arc-like' geochemical signature.||||||
42510|Illbillie granite|23818|5|Briefly described|p43|Ectasian|Ectasian|Age: 1300 Ma (P.A. Arriens, pers. comm.) Geological Province: Musgrave Block.||||||
39575|Inman Arkose|24465|5|Briefly described|p346 Fig.3|||||||||
72786|Innamincka Formation, lower|63056|6|Mentioned|p80|||Informal - see Innamincka Formation. Equivalent to Pando Formation. Geological Province: Warburton Basin.||||||06-FEB-07
79140|Innamincka Granite|65489|5|Briefly described|p84-87|Carboniferous|Carboniferous|[Informal name becoming more widely used in geothermal studies]. Subsurface, high heat producing granites under a blanket of 3.5km sedimentary cover. Has contained pressurised water with output temperatures c.210 degrees C, discovered in Habanero 1 and 2 wells.||||||
67932|Innamincka Red-Beds|44133|6|Mentioned|p33|||See also Innamincka Formation.||||||
29924|Investigator Group|43052|6|Mentioned|Table 5.6|||||||||
80889|Iron Princess beds|71235|5|Briefly described|p6|||Informal subunit of the Corunna Conglomerate derived from Weste (1996). Contains local ore-grade haematite.||Corunna Conglomerate||Overlies the Middleback Subgroup.|Strongly haematised and brecciated conglomerate.|
69739|Jameson Range Troctolite|61341|5|Briefly described|Map legend|||Presented in the compound name Jameson Range Troctolite/Gabbro. Intrusion.||||||21-SEP-05
80332|Janjukian Unit|70660|5|Briefly described|p9, p12, p20, p22, p32|Early Miocene|Chattian|Shown as 'Lower Janjukian Stage' p20 and 'Upper Janjukian unit' p20, 32,   'Lower Janjukian unit' p22, p32.||||Overlies the Ruwarung Member. Overlain by the Point Willunga Formation.|Fossiliferous limestone, silt and sandstone.|05-FEB-18
81419|Janjukian Unit''|70722|5|Briefly described|p218|Late Oligocene|Late Oligocene|Of St. Vincent Basin. Equivalent to Kingscote Limestone Unit K4 of this study.||Unit of Port Willunga Formation.||Uppermost unit of Port Willunga Formation. Underlain by Ruwarung member.||
74091|Kadlunga Shale|61732|5|Briefly described|p28 Fig. 13|Sturtian|Sturtian|Of the Belair Subgroup (Umberatana Group). Geological Province: Adelaide Rift Complex.||||||07-FEB-11
29444|Kalimnan Series""|42966|6|Mentioned|p152|||superseded by Bookpurnong beds.||||||
34327|Kalinjala Mylonite Zone|22629|6|Mentioned|p157,158|Proterozoic|Proterozoic|||||||
34327|Kalinjala Mylonite Zone|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic|Stratigraphic unit is Kalinjala Mylonite.|c.1730-1700 Ma.|||||
69758|Kalka norite/pyroxenite intrusion|44109|4|Described|p10, p44|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Basal pyroxenite zone, (orthopyroxenite, websterite) thick norite zone (norite, minor pyroxenite, gabbro, anorthosite, olivine-bearing norite, olivine websterite). Max. thick: >5000m. ||||||
69758|Kalka norite/pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: >5000m.||||||21-SEP-05
83533|Kalkadoon Donington Supersuite|73525|6|Mentioned|p19 Fig.13|||||||||
69564|Kalkarindji Volcanic Group|65336|4|Described|Map Legend|Early Cambrian|Early Cambrian|Of Georgina Basin [?the volcanics are much more extensive than Georgina Basin - CEB OCT-2010]. Includes Helen Springs Volcanics. Unconformably overlies South Nicholson Group; unconformably underlies Narpa Group. ||||||29-SEP-11
69564|Kalkarindji Volcanic Group|65337|3|Fully described|p61 Table 6, pp94-95.|Early Cambrian|Ediacaran|Encompasses all Early Cambrian continental volcanic rocks in northern Australia. Continental extrusive, high-level intrusive units; sedimentary constituents fluviatile to lacustrine or shallow marine.|||Includes Helen Springs, Antrim Plateau, Colless  Volcanics; Jarong Conglomerate; Kinevans Sandstone; Jindare Formation; Mount Ramsay, Boondawari and Milliwindi dolerites, and more.||Partly vesicular or amygdaloidal tholeiitic basalt, dolerite and andesite; minor trachyte, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits, quartz sandstone, siltstone, conglomerate, sedimentary breccia, limestone, chert.|
69564|Kalkarindji Volcanic Group|67352|5|Briefly described|p30-31|Cambrian|Cambrian|Rawlings et al. (2008). [This name superseded by Kalkarindji Suite] Part of the Kalkarindji Continental Flood Basalt Province, covering a vast area of NT-QLD-WA with an average thickness of .5 km. Various names for exposures include Antrim Plateau, Nutwood Downs, Helen Springs, Peaker Piker, Colless and Table Hill Volcanics.|||Antrim Plateau Volcanics, Colless Volcanics, Table Hill Volcanics, Nutwood Downs Volcanics.|||
69564|Kalkarindji Volcanic Group|69445|6|Mentioned|p30:1, 3|||Kruse in Rawlings et al. (2008); included some components of the Kalkarindji Continental Flood Basalt Province in NT and WA, including minor intercalated sedimentary units. Replaced herein by Kalkarindji Suite.||||||12-JUL-16
69564|Kalkarindji Volcanic Group|69591|6|Mentioned|p54|||Camooweal-Murphy Domain.|||Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72408|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72414|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72415|4|Described|mapsheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Colless Volcanics.|||
69564|Kalkarindji Volcanic Group|72416|4|Described|map sheet|Early Cambrian|Neoproterozoic|Of Geogina Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.|||Includes Colless Volcanics.|||
67933|Kalladeina Formation, Lower|44133|6|Mentioned|p32|||||||||
67934|Kalladeina Formation, upper|44133|6|Mentioned|p33|||||||||
23681|Kanaka Beds|23719|4|Described|p28|Late Eocene|Middle Eocene|See also page 27 Table 8. Overlying unit Melton Limestone. Geological Province: Gawler Craton. Max. thickness 80 m.||||||
23681|Kanaka Beds|39349|6|Mentioned|Map legend|late Eocene|middle Eocene|Middle to Late Eocene||||||
23681|Kanaka Beds|43052|5|Briefly described|Table 2.1|||Late Eocene. Pirie Basin||||||
23681|Kanaka Beds|44133|5|Briefly described|p176|Early Tertiary|Late Eocene|Geological Province: Pirie Basin. Underlies: Melton Limestone. Thickness: 60m. ||||||
23681|Kanaka Beds|67462|5|Briefly described|Map legend.|Late Eocene|Middle Eocene|Pirie Basin.||||||
23681|Kanaka Beds|70334|4|Described|p60|Late Miocene|Middle Eocene|Of Pirie Basin. Thickness: 3-45m on CULTANA, typically 30-40m. Palynological analysis shows age estimates ranging from Middle Eocene to Late Miocene. Depositional environments range from estuarine-lagoonal and lacustrine (Stoian, 2013, pers. comm.; Alley and Lindsay, 1995a).  Intersected in drillholes DH 24205, 24211, 24222, 24251, 24115, 148614-148617.||||Underlain unconformably by Simmens Quarzite or Tapley Hill Formation.|Yellow-brown and grey fine- to medium-grained carbonaceous and lignitic sand with minor clay and clayey sand.|14-OCT-19
23681|Kanaka Beds|71536|6|Mentioned|p3, p18, p20|||Pirie Basin.||||||
67935|Kanaka Beds""|44133|6|Mentioned|p176|||Informal name. See Kanaka Beds. Underlies: Melton Limestone. Thickness: 60m. ||||||
70070|Kangaroo Island Group, Upper|22857|5|Briefly described|p88 Fig. 14.7A|Early Cambrian|Early Cambrian|Informal - see Kangaroo Island Group.||||||
76012|Kangaroo Island Shale|50133|6|Mentioned|p11 Tb.2|||Informal location & sample type description?||||||
42511|Kangaroo Island granites|23818|6|Mentioned|p107|||||||||
81341|Kangaroo Island red beds|70031|6|Mentioned|p250|||ca 515 Ma age given in table for late Cryogenian to post-Delamerian Orogeny poles. See p250 Table 2 for paleomagnetic analysis.||||||08-AUG-19
76827|Kangaroo Island redbeds|67030|6|Mentioned|p412 Fig. 7, p413 Tb. 2|Cambrian|Cambrian|Magnetic information presented for comparison (Klootwijk 1980). Abbreviated as Kangaroo Is red beds in p413 Tab. 2||||||26-APR-12
39214|Kanmantoo Bluestone|23731|6|Mentioned|p27|||Of Tapanappa Formation. Commercial name for quarried 'bluestone' rock.||||||
39214|Kanmantoo Bluestone|60566|5|Briefly described|p28-29|||Comercial name for micaceous siltstone known as bluestone in SA. Not intended as a formal name.||||||
39214|Kanmantoo Bluestone|61237|5|Briefly described|p36|Cambrian|Cambrian|Commercial name for building stone quarried from the Tapanappa Formation for walling and paving stone.||||||16-AUG-05
78191|Kanmantoo Formation|68822|6|Mentioned|p324|||Deepwater depositional environment.||||Underlain by the Normanville Group.||
42224|Kanmantoo Group schist|24361|6|Mentioned|p51|||Informal - see the Kanmantoo Group.||||||09-MAR-05
69043|Kanmantoo Group, Lower|60712|5|Briefly described|p31 Fig. 4|Early Cambrian|Early Cambrian|Informal - see Kanmantoo Group.||||||
67937|Kanmantoo Group, Upper|44133|5|Briefly described|p18|||Informal, see Kanmantoo Group.||||||
67936|Kanmantoo Group, lower|44133|6|Mentioned|p15|||Informal, see Kanmantoo Group.||||||
67936|Kanmantoo Group, lower|60712|6|Mentioned|p27, p37|Early Cambrian|Early Cambrian|Informal - see Kanmantoo Group.||||||
40344|Kanmantoo Shale|23932|5|Briefly described|p680 Fig. 8|Early Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
29925|Kanmantoo complex""|43052|6|Mentioned|p20|||||||||
34552|Kanmantoo metasediments|22773|5|Briefly described|Fig24.5p350|Cambrian|Adelaidean|||||||
34552|Kanmantoo metasediments|22857|6|Mentioned|p350 Fig.24.5|Adelaidean|Adelaidean|Informal name. Geological Province: Adelaide Fold Belt, Kanmantoo Fold Belt. ||||||
34552|Kanmantoo metasediments|22887|5|Briefly described|Fig.5 p12|Cambrian|Adelaidean|Kanmantoo Fold Belt.||||||
76007|Kanmantoo shales|50133|6|Mentioned|p1||Paleozoic|Probably informal reference to shales in units of the Kanmantoo Group. See also Table 2 p11.  ||||||
69940|Kanmantoo turbidite fans|60904|6|Mentioned|p806 Fig. 25b|||Informal term for turbidites of the Kanmantoo Group. ||||||
28635|Kapunda carbonates|36953|6|Mentioned|p102|||||||||
26654|Karinya Shale Member|23818|6|Mentioned|p105|||Of the Brukunga Formation.||||||
26654|Karinya Shale Member|30801|6|Mentioned|p5|||Brukunga Formation. Table P5-6||||||
26654|Karinya Shale Member|33471|6|Mentioned|p557|||||||||
26654|Karinya Shale Member|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Lower - Middle Cambrian||||||
26654|Karinya Shale Member|34612|5|Briefly described|p105|||||||||
26654|Karinya Shale Member|41947|5|Briefly described|p21|||||||||
26654|Karinya Shale Member|60712|6|Mentioned|p33|Early Cambrian|Early Cambrian|Elevated to formation status by Gatehouse (1988) as Karinya Shale. Previously of the former Brukunga Formation on ADELAIDE sheet.||||||31-MAY-05
39568|Karinya Shale""|24465|4|Described|p355|Early Cambrian|Early Cambrian|Informal name - see Karinya Shale.||||||
73493|Karlaya Limestone Member|63397|2|Defined|30-31|Neoproterozoic III|Neoproterozoic III|Of the Tanana Formation. Type section in text. Limestone with thin silty mudstone interlayers. Thickness: 107m. Overlies Dey-Dey Mudstone.||||||03-FEB-11
83060|Karoonda Palaeosol|73188|5|Briefly described|p314, p338, p346|||Of Firman, 1966. [Not strictly a stratigraphic unit]. Refers to the silicified and ferruginised surface developed on the Pliocene Parilla Sand in the Murray Basin. [Possibly] within the Kurrajong Formation type section east of Willunga. [See also Karoonda Paleosol p351].|||||Matrix-supported silica and iron-cemented sandy pebble beds[?].|
28636|Karoonda Soil|42717|5|Briefly described|map legend|Pliocene||Variation on Karoonda Paleosol.||||||
28636|Karoonda Soil|43073|5|Briefly described|p17|||||||||
73190|Karronda Surface|61896|6|Mentioned|p45|Cenozoic|Cenozoic|On the shoreline ridges of the Murray Basin. Name probably misspelt - place name is Karoonda.||||||19-DEC-07
76878|Katjiitara Formation|67462|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Tirari Sub-basin, Lake Eyre Basin.||||||
76885|Katnook Sandstone Member|61547|6|Mentioned|p461 Fig.2, p471, p473. |Hauterivian|Hauterivian|See Katnook Sandstone.||||Overlies the Laira Formation.||
78682|Katnook sandstone|67541|6|Mentioned|p79, p86|||Results of this study indicate that sandstones such as the Katnook sandstone can efficiently store CO2.||||||
76211|Kenella Paragneiss|64722|5|Briefly described|p12||Neoarchean|Contains 2720-2650 Ma detrital zircons.||||||
76211|Kenella Paragneiss|67058|5|Briefly described|p476, p492.|Neoarchean|Neoarchean|Central Gawler Craton.|c.2530 Ma.|Unit in Mulgathing Complex.||||
76211|Kenella Paragneiss|67980|6|Mentioned|p561 Tb.3, p564|Siderian|Siderian|Christie Domain, Gawler Craton. Igneous crystallisation age by Jagodzinski et al. (2009). Appears as Kenella Gneiss in Tb.3.|2474 +/- 4 Ma (U-Pb SHRIMP zircon).|||||
68705|Kenella gneiss|60704|6|Mentioned|p697|Archean|Archean|Informal - see Kenella Gneiss.||||||07-NOV-08
83517|Kennedy's Dam Group|73155|5|Briefly described|p274, p277, p282 Fig.13, p283-285|||Mount Woods Domain, southeast parts of Southern Geophysical Zone, is not exposed. Similar geophysical signature to metasediments, predominantly low magnetic response and smooth texture, intercalated with marker horizons. May be equivalent to Skylark Metasediments and Blue Duck Group sedimentary packages. Interpreted to occupy region between upper and lower plates of the Mount Woods Metamorphic Core Complex, between the central Mount Woods Metamorphics and outer Skylark Metamorphics. Misspelt as Kennedy's Dam Metamorphics p274? Proterozoic age inferred.|||||Gneissic units including calc-silicates and amphibolites.|05-SEP-22
83516|Kennedy's Dam Metamorphics|73155|6|Mentioned|p274|||May be broadly equivalent with Skylark Metamorphics. See also Kennedy's Dam Group.||||||
39569|Keynes subgroup|24465|6|Mentioned|p358|||Informal - see Keynes Subgroup.||||||
34824|Kin Gunnia Calc-Silicate Member|22960|5|Briefly described|p91||Paleoproterozoic|Misspelling of the King Gunnia Calc-Silicate Member.||||||10-SEP-19
42225|Kinchina Quarry pegmatites|24361|5|Briefly described|p51|Early Ordovician|Early Ordovician|Infromal. Name refers to locality in which pegmatites are found. Age: 478+/-6 Ma.||||||
30610|Kingoonya granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
34723|Kingston Blue Granite|22848|5|Briefly described|p35|||Informal name for commercial dimension stone - now formalised to Taratap Granodiorite. Actually written as "KIngstone Blue Granite".||||||08-DEC-08
29438|Knight Beds""|22799|6|Mentioned|p25|||||||||
29438|Knight Beds""|42966|6|Mentioned|p96|||Refers to Firman (1973).||||||
29439|Knight Formation""|42966|6|Mentioned|p96|||Refers to Harris (1966).||||||
29464|Knight beds|42966|5|Briefly described|p407|||Now Renmark Group.||||||
70620|Koeris metabasalts|62373|6|Mentioned|p510 Fig.5, p516|||Not intended as a formal name - related to the suite of metabasite groups in the Curnamona Province.||||||
30606|Kokatha Suite|50537|6|Mentioned|p1.1, 3.1|||I-Type. Of the Hiltaba Supersuite.||||||
41683|Kokatha granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Part of Kokatha suite. Age: 1592Ma.||||||07-FEB-11
41683|Kokatha granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
41684|Kokatha suite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Includes Kokatha, Kychering, Kingoonya, Tarcoola, Minnipa, Wudinna and Buckleboo granites. Age: 1592Ma.||||||07-FEB-11
41684|Kokatha suite|50605|5|Briefly described|p(ii), 1.3, 8.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||
41684|Kokatha suite|65390|5|Briefly described|p27|Calymmian|Calymmian|Said to be of Budd et al. (1998) [NB: 'Kokatha type' used, not 'Kokatha suite']. Of the Hiltaba Suite. Less fractionated (than the Olympic Dam Suite) and generally related to Au, Ag and base metal systems. May be equivalent to 'Granite, Kokotha' on p26.||||||
28650|Kongerong Formation|33224|6|Mentioned|p69|||Palynology||||||
23702|Konkoby Basalt|39905|5|Briefly described|Fig.4|||Check spelling: Konkaby used on Kingoonya sheet.||||||
67959|Kooliata Coal Member|44133|5|Briefly described|p164, 152 Fig. 10.2|Oligocene|Eocene|Of the Clinton Formation. Geological Province: Saint Vincent Basin. Thickness: 20m.||||||
34788|Koolywurtie Member|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
34788|Koolywurtie Member|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Parara Limestone.  Geological Province: Stansbury Basin.||||||19-JAN-05
34788|Koolywurtie Member|44133|5|Briefly described|p4 Fig. 7.2, 6, 12|Early Cambrian|Early Cambrian|Geological Province: Stansbury Basin. Of the Parara Limestone. Maximum Thickness: 70m.||||||
34788|Koolywurtie Member|60990|5|Briefly described|p83 |||Yorke Peninsula. Biogeographic correlation with Cymbric Vale Formation.||Parara Limestone||||
34788|Koolywurtie Member|65375|4|Described|p27 Fig.5, p29. |Cambrian|Cambrian|Formal name is Koolywurtie Limestone Member. Formed a reefal complex in Parara Limestone.||Unit in Parara Limestone.||Locally unconformably overlain by Minlaton Formation.|Archaeocyath-algal bioherms.|
34788|Koolywurtie Member|65686|5|Briefly described|p412, 413|||Contains first archaeocyaths discovered in Australia (Tepper 1879).||Of the Parara Limestone.||||07-MAY-12
34788|Koolywurtie Member|66761|5|Briefly described|p254, 255|Cambrian|Cambrian|Yorke Peninsula. Of the Parara Limestone. Correlated in part with Heatherdale Shale and Mount McDonnell Formation.||||||14-MAR-12
34788|Koolywurtie Member|68735|6|Mentioned|p232, p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||Parara Limestone.|||Carbonate-dominated.|10-APR-17
34788|Koolywurtie Member|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||Of the Parara Limestone.||||
34788|Koolywurtie Member|70833|5|Briefly described|p200|Cambrian|Cambrian|Of Western Stansbury Basin. Includes D. odyssei zone.||Unit of Parara Limestone.||Occurs in upper part of Parara Limestone.||
34788|Koolywurtie Member|73247|6|Mentioned|p205|Cambrian (Stage 4)|Cambrian (Stage 3)|[Variation of established name? Probably an abbreviation of Koolywurtie Limestone Member].||||Equivalent to Mount McDonnell Formation.||
27451|Koonunga Phospherite Member|34536|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
27451|Koonunga Phospherite Member|41639|6|Mentioned|p12|||||||||
77227|Kooringa Limestone Member|66522|6|Mentioned|p19.|Neoproterozoic|Neoproterozoic|Name reserved with Australian Stratigraphy Commission. See Kooringa Member.||||||
69655|Kootaburra Formation|61155|5|Briefly described|p17|Pleistocene|Pleistocene|Overlies the Katipiri Formation. Age: <1.5Ma. Geological Province: Lake Eyre Basin.||||||
29908|Kulgera Adamellite""|43052|6|Mentioned|p162|||Refers to Wilson (1960).||||||09-OCT-06
29912|Kulgera Dyke Swarm""|43052|6|Mentioned|p165|||Synonym for Alcurra Dyke Swarm||||||
29907|Kulgera Suite|23483|6|Mentioned|p5 Fig 1|||||||||
29907|Kulgera Suite|24496|4|Described|p14, 16|Mesoproterozoic|Mesoproterozoic|Age: 1186+/-10 - 1120 Ma. Felsic plutons - adamellite to diorite, commonly charnockite. Some "intrusives" may be charnockite overprints of Birksgate Complex gneisses. Equivalent to Umutja Suite.  Geological Province: Musgrave Block.||||||
29907|Kulgera Suite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1200-1150Ma.  Geological Province: Musgrave Block.||||||11-MAY-05
29907|Kulgera Suite|43052|4|Described|p162|||||||||
29907|Kulgera Suite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granitoids of Musgravian Orogeny.||||||26-MAY-05
29907|Kulgera Suite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29907|Kulgera Suite|43298|5|Briefly described|Map Legend||Mesoproterozoic|||||||
29907|Kulgera Suite|50607|6|Mentioned|p1.2, 3.3|||||||||
29907|Kulgera Suite|60683|5|Briefly described|p12|Mesoproterozoic|Mesoproterozoic|Felsic intrusion named by Major and Conor (1993).  Geological Province: Musgrave Block.||||||20-APR-05
29907|Kulgera Suite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1198-1175Ma; ~1300Ma? Dominantly post orogenic granitoids. Probably includes some foliated granitoids pre- and post-dating an early orogenic phase ~1300Ma.||||||
29907|Kulgera Suite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Dominantly post-orogenic granitoid rock, mainly adamellite. Probably includes some foliated granitoid rock pre- and post-dating and early orgenic phase ~1300 Ma. Age: 1198-1175 Ma; ~1300 Ma?||||||
29907|Kulgera Suite|61154|6|Mentioned|p42 Appendix|||Superseded by Kulgera Supersuite and then by Kulgera Granite. Synonymous with Pitjantjatjara Supersuite - as an informal reference to its granites (Major and Conor 1993). Geological Province: Musgrave Block.||||||
29907|Kulgera Suite|65309|4|Described|pp5-7.  |||Volumetrically extensive sheets, veins, stocks and dykes of granitic rocks intruding basement gneiss of Musgrave Block.|1190-1120 Ma.||||Granite, leucogranodiorite, quartz monzonite, porphyritic granite, leucosyenite and microgranite.|16-JAN-15
29907|Kulgera Suite|65376|6|Mentioned|p247 Fig.6.57.|Mesoproterozoic|Mesoproterozoic|||||||
29907|Kulgera Suite|67375|6|Mentioned|p150.|Mesoproterozoic|Mesoproterozoic|Of Major and Conor, 1993. Subsequently the Pitjantjatjara Supersuite.||||||
33040|Kulgera Supersuite|24197|5|Briefly described|p26, p97-98|Mesoproterozoic|Mesoproterozoic|Incl: Kulgera Suite, Pottuyu Granitic Cmplx, Olia Gneiss. Composed of widespread felsic, mainly monzogranitic and charnockite plutons. Age:1190Ma.Together with Winburn Suite intrudes Birksgate Complex. Geol.P: Musgrave Block. Eg.of Cullen Association.||||||07-FEB-11
33040|Kulgera Supersuite|50607|5|Briefly described|p1.1, 2.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Age: 1190-1150Ma.||||||
33040|Kulgera Supersuite|61154|5|Briefly described|p42 Appendix|||Superseded Kulgera Suite; but is itself now superseded by Kulgera Granite. Synonymous with Pitjantjatjara Supersuite - as an informal reference to its granites (Budd et al 2002). Geological Province: Musgrave Block.||||||05-AUG-05
33040|Kulgera Supersuite|63866|6|Mentioned|p205-p207, p214|||Musgrave Province.||||||
33040|Kulgera Supersuite|65256|6|Mentioned|p7|Stenian|Mesoproterozoic|Granites.||||||
72813|Kulpara Formation, upper|23981|6|Mentioned|p38, p59|||Informal - see Kulpara Formation.||||||
72814|Kulpara limestone|23981|6|Mentioned|p13|||Informal and suiperseded - see Kulpara Formation.||||||
42421|Kultpittaja Granite Complex|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Age: 1190-1130 Ma. Equivalent to Pottyu Suite. Geological Province: Musgrave Block.||||||21-DEC-04
34766|Kulyong Formation|22922|5|Briefly described|34|||||||||
34766|Kulyong Formation|23282|2|Defined|p79|Late Cambrian|Middle Cambrian|Age: Middle to Late Cambrian 507 - 505Ma. Defined by Major and Teluk (1967) as Kulyong Volcanics. Jackson & van de Graff (1981) suggest that the Kulyong Volcanics and Table Hill Volcanics are synonyms, Therefore changed to formation. Of Officer Basin.||||||21-JUL-09
34766|Kulyong Formation|24112|5|Briefly described|p254 Fig.2|Late Cambrian|Middle Cambrian|Geological Province: Officer Basin||||||
34766|Kulyong Formation|62570|5|Briefly described|p580 Figs. 2 and 3|Late  Cambrian|Late Cambrian|Geological Province: Officer Basin. Tholeiitic basalt.||||||10-AUG-07
34766|Kulyong Formation|64970|6|Mentioned|p719 Fig. 2|Cambrian|Cambrian|Geological Province: Officer Basin.||||||27-MAY-09
34766|Kulyong Formation|66521|4|Described|p20.|||Named by Morton and Drexel (1997) to  replace Kulyong Volcanics, to include 8 m of sediment below the 3 m thick basalt unit. Thicker and more widely distributed in Western Australia, hence renamed Table Hill Volcanics as it is known in that State.|K-Ar ages of 485 +/- 20 Ma and 475 +/- 20 Ma.||||Basalt; sediments.|
34766|Kulyong Formation|69445|5|Briefly described|p30:5-6, 17|||Officer Basin. Western-central SA. Superseded by Table Hill Volcanics.||||Overlies Trainor Hill Sandstone. Is overlain by Mount Chandler Sandstone.||12-JUL-16
34766|Kulyong Formation|72478|6|Mentioned|p8|Late Cambrian|Middle Cambrian|Officer Basin.|c. 507 -495 Ma|||Unconformably overlies the Trainor Hill Sandstone. Overlain by the Mt Chandler Sandstone.||
35701|Kulyong Formation""|23282|6|Mentioned|p80|||||||||
30611|Kychering Granite|64137|6|Mentioned|p1553-1555|||Neodymium and lead isotope data.||||||
30611|Kychering Granite|65390|6|Mentioned|p22 Fig. 3|Calymmian|Calymmian|Wilgena Domain, Gawler Craton.||||||
30611|Kychering Granite|66302|6|Mentioned|p46|Calymmian|Calymmian|Informal name. Wilgena Domain. |1590 to 1575 Ma (Budd, 2006)|Hiltaba Suite|||Granite.|
30611|Kychering Granite|71236|6|Mentioned|p24|||||||||
30611|Kychering Granite|72065|5|Briefly described|p105|Ectasian|Ectasian|Geological province: Gawler Craton. Emplacement age at 1375.7+\-4.3 Ma (zircon, U-Pb, LA-ICP-MS, Budd, 2006).||Unit of Hiltaba Suite.||||
41685|Kychering granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Of the Kokatha suite. Age: 1592Ma.||||||07-FEB-11
41685|Kychering granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
80625|Labrynth Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton.|ca 1775 Ma||||Sandstone, greywacke.|
41686|Lacy Island granite|50605|5|Briefly described|p7.18|Paleoproterozoic|Paleoproterozoic|Of the Saint Peter Suite. Geological Province: Gawler Craton & Curnamona Province.||||||07-NOV-08
68706|Lady Jane Diorite""|60704|6|Mentioned|p688|||Informal - see Lady Jane Diorite||||||
70621|Lady Louise Suite metabasites|62373|6|Mentioned|p511|||Informal - see Lady Louise Suite.||||||
79050|Lake Everard Volcanic Complex|69649|6|Mentioned|p25|Mesoproterozoic|Mesoproterozoic|[misspelling of Glyde Hill Volcanic Complex - see p16] The dykes of the Moonamby Dyke Suite are said to only occur along the western margin of the Lake Everard Volcanic Complex.||||||26-FEB-15
77085|Lake Eyre Formation|62592|5|Briefly described|p18.|Tertiary|Tertiary|Thin sedimentary cover, hosting roll-front uranium deposits including Honeymoon, Goulds Dam and Beverley.||||||
40371|Lake Frome Group, Lower|24334|5|Briefly described|p48 Tb.1|Middle Cambrian|Early Cambrian|Age: 505 - 514 Ma||||||
40373|Lake Frome Group, Upper|24334|5|Briefly described|p48 Tb.1|Late Cambrian|Middle Cambrian|Age: 495 - 505 Ma||||||
77794|Lake Gilles leucogranite|65915|4|Described|p6-9, p13-16|Neoarchean|Neoarchean|Informal name? Outcrops along N shore of Lake Gilles. Formerly mapped as undifferentiated gneissic granite and granitic gneiss of Lincoln Complex. Dykes of leucogranite ~30 cm to several m wide. Even-grained. Dominated by quartz and K-feldspar, with steeply dipping foliation defined by grey quartz ribbons. SHRIMP U-Pb zircon age of 2529 +/-4 Ma. Geochemical analyses detailed.||||||
77794|Lake Gilles leucogranite|68208|6|Mentioned|p31 Fig.2, p39||Neoarchean|Informally named, Sleaford Complex aged.|Crystallisation age ~2540 Ma.|||||
77794|Lake Gilles leucogranite|71349|6|Mentioned|p738|||Gawler Craton. Generated from melting of a c.3.2 Ga source (Fraser et al., 2010).||||||
39297|Lake Harris komatiite|24287|6|Mentioned|p31|||Informal name.||||||
82107|Lake Ifould Granite|72459|5|Briefly described|p22|Palaeoproterozoic|Palaeoproterozoic|Christie Subdomain of the Gawler Craton. Intepreted to be of the Ifould Magmatic event.|1672 +/- 17 Ma (Teasdale, 1997)|||||
76766|Lake Ifould Suite|64722|5|Briefly described|p14|Siderian|Siderian|See Ifould Suite. Samples of this suite have been dated at 2436 +/-14 Ma.||||||
76766|Lake Ifould Suite|65772|6|Mentioned|p234 Fig.8, p238|||Also called Ifould Suite (Fig.12) and "Tunkillia Suite (or Ifould Suite/Complex)"(p238). Major element chemistry, and low- to medium-K lithologies, distinguish this unit from Tunkillia Suite.||||||
79134|Lake Phillipson beds|69946|6|Mentioned|p2|||Ludbrook (1967). Recognised in Lake Phillipson Bore. Informal name, replaced by Boorthanna Formation (Townsend and Ludbrook, 1975).||||||
77398|Lake Tallacootra Aplite|65376|6|Mentioned|p186.|||Not a formal name; used (Teasdale 1997) to identify an aplite sample used for zircon dating.||||||
79079|Lamdina Formation""|42008|6|Mentioned|p266|Late Triassic|Late Triassic|Discussed as one of a group of 'previous names' for Late Triassic strata ('Beanbush Beds', 'Morney Beds', 'Upper Triassic Unit' ), now all included in Cuddapan Formation.||||||09-APR-15
36820|Langra Conglomerate|23858|5|Briefly described|p916|Late Devonian|Middle Devonian|Of Finke Group. Overlain by Horeshoe Bend Shale; underlain by Polly Conglomerate. Geological Province: Amadeus Basin.||||||13-OCT-06
67960|Le Hunt Formation|44133|6|Mentioned|p230|||Of the Saint Kilda Formation. Same as Le Hunte Formation.||||||
68747|Le Hunte Member|60958|5|Briefly described|Map Legend|Holocene|Holocene|Of the Saint Kilda Formation.  Gypsiferous lacustrine sediment of coastal saline lakes.||||||23-DEC-09
68747|Le Hunte Member|61070|6|Mentioned|Map Legend|Quaternary|Quaternary|||||||12-JAN-10
68747|Le Hunte Member|61121|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Gypsiferous lacustrine sediment of coastal saline lakes; carbonate sand with gastropod fossiles, venered by yellow siliceous sand; stromatolites; basal part with seagrass 'Posidonia'.||||||07-JUN-05
68747|Le Hunte Member|64282|5|Briefly described|Map legend|Holocene|Holocene|Of the Saint Kilda Formation. Gypsiferous lacustrine sediment of coastal saline lakes, carbonate sand with gastropod fossils, veneered by yellow siliceous sand; stromatolites; basal mud with seagrass 'Posidonia'.||||||23-DEC-09
68747|Le Hunte Member|65375|5|Briefly described|pp42-43.|Holocene|Holocene|Gypsiferous, lacustrine, coastal saline lake deposit.||Unit in Saint Kilda Formation.|||Laminated gypsum, rhythmically layered, up to 2m thick, with domal stromatolites; aeolian gypsum, unconsolidated, mixed with clay and sand.|
68747|Le Hunte Member|68131|6|Mentioned|p7, p17|Holocene|Holocene|Yorke Peninsula.||||||
68747|Le Hunte Member|70337|5|Briefly described|Map legend.|Holocene|Holocene||||||Gypsiferous lacustrine sediment of coastal saline lakes.|
68747|Le Hunte Member|73107|5|Briefly described|Map legend.|Holocene|Holocene||||||Gypsiferous lacustrine sediment of coastal saline lakes. Carbonate sand with gastropod fossils, veneered by yellow siliceous sand. Stromatolites. Basal mud with seagrass Posidonia.|
74089|Leemurra Mudstone|61732|5|Briefly described|p63|||Informal name for a shale unit in middle of the Tanan Formation. Not recognised regionally.||||||07-FEB-11
32079|Leigh Coal Measures|43923|6|Mentioned|p1|||||||||
76914|Lincoln Batholith|65375|5|Briefly described|p45 Table 8.|||Presumably a variation on Lincoln Complex, which itself is not in use. Yorke Peninsula.|Emplaced c.1920-1860 Ma.|||||
28681|Lincoln Complex|22494|6|Mentioned|p35|||||||||
28681|Lincoln Complex|22613|4|Described|p11|Paleoproterozoic|Paleoproterozoic|Gawler Craton||||||07-NOV-08
28681|Lincoln Complex|22614|5|Briefly described|map|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|22629|4|Described|fig2p147,157|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|22635|6|Mentioned|p493||Statherian|||||||
28681|Lincoln Complex|22643|5|Briefly described|p183, fig3p187|||||||||
28681|Lincoln Complex|22668|5|Briefly described|p4|Orosirian|Orosirian|1850Ma||||||
28681|Lincoln Complex|22690|6|Mentioned|P312|||||||||
28681|Lincoln Complex|22796|5|Briefly described|p76|||||||||
28681|Lincoln Complex|23481|5|Briefly described|p19 Fig 1|||Geological Province: Gawler Craton.||||||
28681|Lincoln Complex|23482|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|23719|4|Described|p19|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
28681|Lincoln Complex|23803|5|Briefly described|p28|||Geological Province: Gawler Craton.||||||
28681|Lincoln Complex|23805|5|Briefly described|p4 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
28681|Lincoln Complex|24261|5|Briefly described|p1047 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: >1600Ma. Geological Province: Gawler Craton||||||07-NOV-08
28681|Lincoln Complex|24360|5|Briefly described|p53|Paleoproterozoic|Paleoproterozoic|Geological Province: Yorke Peninsula, Gawler Craton||||||07-NOV-08
28681|Lincoln Complex|24422|5|Briefly described|p84 Fig. 1, p86|Paleoproterozoic|Paleoproterozoic|Age: ca. 1845-1730 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
28681|Lincoln Complex|24526|6|Mentioned|p99|||Name replaced by Lincoln Batholith in this study, but not a formal name.||||||
28681|Lincoln Complex|24597|5|Briefly described|p526 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca1850-1730Ma.  Intruded the Hutchison Group.  Geological Province: Gawler Craton.  See also p526.||||||07-NOV-08
28681|Lincoln Complex|37461|6|Mentioned|Fig.5.2|||||||||
28681|Lincoln Complex|37620|6|Mentioned|p7|||||||||
28681|Lincoln Complex|37811|6|Mentioned|p222|||||||||
28681|Lincoln Complex|39345|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28681|Lincoln Complex|39353|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|39802|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|39842|6|Mentioned|Fig.1|||||||||
28681|Lincoln Complex|39844|6|Mentioned|p62|||||||||
28681|Lincoln Complex|39949|6|Mentioned|p273|||||||||
28681|Lincoln Complex|40227|6|Mentioned|p44|||||||||
28681|Lincoln Complex|40430|6|Mentioned|p7|||See also Table.2||||||
28681|Lincoln Complex|40448|5|Briefly described|p34|||Also mention on p25.||||||02-JUN-09
28681|Lincoln Complex|40644|5|Briefly described|p120 Fig. 2, p121, p124 Fig. 3|Mesoproterozoic|Paleoproterozoic|Of Thomson (1980). For granitoids of the Kimban Orogeny of 1820-1580Ma. Includes Donington Granitoid Suite, unrecognisable remnants of Hutchinson Group, remobilised Sleaford Complex rocks and other unnamed granites.||||||07-NOV-08
28681|Lincoln Complex|41125|6|Mentioned|p30|||See also P42||||||
28681|Lincoln Complex|41239|4|Described|p95|||||||||
28681|Lincoln Complex|41325|6|Mentioned|Fig.2|||||||||
28681|Lincoln Complex|41327|6|Mentioned|Fig.2|||||||||
28681|Lincoln Complex|41493|6|Mentioned|Table 1|||||||||
28681|Lincoln Complex|41609|6|Mentioned|p125|||||||||
28681|Lincoln Complex|41619|6|Mentioned|Map legend|Tertiary||||||||
28681|Lincoln Complex|41667|6|Mentioned|p22|||||||||
28681|Lincoln Complex|41972|6|Mentioned|Fig.1 P364|||||||||
28681|Lincoln Complex|41973|5|Briefly described|p387|||||||||
28681|Lincoln Complex|42102|6|Mentioned|p85|||||||||
28681|Lincoln Complex|42167|6|Mentioned|Fig.4 P117|||||||||
28681|Lincoln Complex|42291|6|Mentioned|p2|||||||||
28681|Lincoln Complex|42357|6|Mentioned|p8|||||||||
28681|Lincoln Complex|42465|5|Briefly described|Map Legend|||||||||
28681|Lincoln Complex|42466|5|Briefly described|Map Legend|||||||||
28681|Lincoln Complex|42468|5|Briefly described|Fig. 1 P2|||||||||
28681|Lincoln Complex|42469|4|Described|p12|||||||||
28681|Lincoln Complex|42475|5|Briefly described|p10|||||||||
28681|Lincoln Complex|42546|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28681|Lincoln Complex|42716|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
28681|Lincoln Complex|42736|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
28681|Lincoln Complex|42738|5|Briefly described|map legend|Mesoproterozoic||||||||
28681|Lincoln Complex|42816|5|Briefly described|p12|||||||||
28681|Lincoln Complex|42903|6|Mentioned|p423|||||||||
28681|Lincoln Complex|43049|5|Briefly described|p12|||||||||
28681|Lincoln Complex|43052|4|Described|p74,Table 4.4|||||||||
28681|Lincoln Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Orogenic granitoids: gneiss and migmatite, foliated and non-foliated granitoids. Geological Province: southern Gawler Craton.||||||07-NOV-08
28681|Lincoln Complex|43071|5|Briefly described|p12|||||||||
28681|Lincoln Complex|43141|6|Mentioned|p63,Fig.1|||||||||
28681|Lincoln Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|43561|6|Mentioned|p1438|||||||||
28681|Lincoln Complex|43595|4|Described|p354||Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|43839|6|Mentioned|p29, Fig2 p30|||Now considered to be deformed Hiltaba Suite granite||||||12-JUL-16
28681|Lincoln Complex|44695|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28681|Lincoln Complex|50605|5|Briefly described|p3.1, 5.1|||Of the Younger Lincoln Supersuite. Geological Province: Gawler Craton & Curnamona Province.||||||
28681|Lincoln Complex|60484|6|Mentioned|p32|||Geological Province: Gawler Craton.||||||
28681|Lincoln Complex|60657|5|Briefly described|p13 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1850Ma. Geological Province: Gawler Craton.||||||07-NOV-08
28681|Lincoln Complex|60848|5|Briefly described|p153|Mesoproterozoic|Mesoproterozoic|Orthogneisses and granites.  Age: 1850-1750Ma.||||||23-JUL-13
28681|Lincoln Complex|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1853-1692Ma. Syntectonic to late tectonic granitoids, minor basic intrusives, Kimban Orogeny.||||||07-NOV-08
28681|Lincoln Complex|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated Lincoln Complex: syntectonic to late tectonic granitoid rock and minor basic intrusive rock, Kimban Orogeny. Age: 1853-1692 Ma.||||||07-NOV-08
28681|Lincoln Complex|61307|5|Briefly described|p61 Fig. 27|||Pre, syn-tectonic gneissic granitoids and metabasics +/- mylonite.||||||
28681|Lincoln Complex|62893|4|Described|Map Legend, p10, p13, p25, p28, p38|Early Proterozoic|Early Proterozoic|Syn-orogenic (Kimban Orogeny) granite intrusive bodies; complex relationship of intrusions.|||Carappee Granite|Intrudes Hutchison Group.|Massive to foliated, cream, pink, and grey granite, granitic gneiss, migmatitic gneiss, aplite and pegmatite with minor mafic intrusives including fine-grained dolerite dykes; intense chloritic alteration in some places.|
28681|Lincoln Complex|62898|6|Mentioned|p200|Paleoproterozoic|Paleoproterozoic|Includes St Peter Suite.  Age: 1620+/-4Ma.||||||07-NOV-08
28681|Lincoln Complex|64281|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|Forms a crystalline basement on coastal Yorke Peninsula, Althorpe Islands and northern Kangaroo Island, South Australia. More a structural complex than stratigraphical unit.||||||23-DEC-09
28681|Lincoln Complex|64313|6|Mentioned|p450|||The Donington Suite was formerly included in the Lincoln Complex but now excluded due to revision based on timing and duration of the Kimban Orogeny.||||||09-FEB-10
28681|Lincoln Complex|65219|6|Mentioned|p26|Paleoproterzoic|Paleoproterzoic|Formerly included Donington Suite.||||||22-SEP-09
28681|Lincoln Complex|65221|5|Briefly described|p26, 27, p28 Fig.3|Palaeoproterozoic|Palaeoproterozoic|Some outcrops previously assigned to this unit may be reassigned. ||||||
28681|Lincoln Complex|65375|6|Mentioned|p8, p44. |Paleoproterozoic|Paleoproterozoic|Name not used as a stratigraphic term. Said to contain Donington and Moody Suites.||||||
28681|Lincoln Complex|65376|6|Mentioned|p11.|||Obsolete term for magmatic rocks on Eyre Peninsula.||||||
28681|Lincoln Complex|65390|6|Mentioned|p20|||Parker, 1993. Wilson (1999) proposed the term "Lincoln Orogeny" for the c.1850 Ma first stage of the Kimban Orogeny; confusion with this unit leads these authors to propose the term Neill Event.||||||
28681|Lincoln Complex|65915|5|Briefly described|p5-6, p11|||Superseded term encompassing Donington Suite and syn-Kimban intrusives.||||||
28681|Lincoln Complex|65922|5|Briefly described|p9, p14 Tb.1, p15-16, p29 Fig. 6|Statherian|Orosirian|This name is expected to fall into disuse as other names replace it; eg Donington Suite. Gawler Craton. Syn-Kimban Orogeny (~1850-1710 Ma). Not dated on this map sheet. Includes Donington Suite, Moody Suite. Pinkish coloured, medium-grained granite; foliated biotite granite; massive weakly foliated leucogranite. Intrudes Archean to earliest Proterozoic gneiss.||||||
28681|Lincoln Complex|66843|5|Briefly described|p34|||Eyre Peninsula, S.A. Mentioned as the source of a QGNG standard for SHRIMP geochronology.|1849.8 +/- 1.1 Ma.||||Includes quartz gabbronorite.|
28681|Lincoln Complex|67536|6|Mentioned|Map Legend|||Gawler Craton.||||||
28681|Lincoln Complex|68131|6|Mentioned|p57|Paleoproterozoic|Paleoproterozoic|||||||
28681|Lincoln Complex|68158|5|Briefly described|p4||||||Burkitt Granite; local relict schist and amphibolite of the Hutchison Group.||Syntectonic granitoids: granite, pegmatite, gneiss, schist and amphibolite; gneissic granite and granitic gneiss; gabbroic and amphibolite intrusives.|
28681|Lincoln Complex|68208|6|Mentioned|p32|||Of Weste (1996). Included Cooyerdoo Granite outcrops as part of undifferentiated granitoids.||||||
28681|Lincoln Complex|68714|6|Mentioned|p17 Fig.7|||||||||
28681|Lincoln Complex|70721|5|Briefly described|p63, p72-p73|||Originally conceived to describe intrusive rocks associated with the Kimban Orogeny and included the Donington Suite, Colbert Granite, Moody Suite, Wertigo Granite, Middle Camp Granite and Carappee Granite.||||||
28681|Lincoln Complex|71317|5|Briefly described|p19|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton. This name is now obsolete and basement rocks formerly assigned to it are now included in the Pinbong Suite.||||||
28681|Lincoln Complex|71859|4|Described|p1-p2, p14, p29, p35-p36|Paleoproterozoic|Paleoproterozoic|Gawler Craton. The Minbrie Gneiss and Carpa Granites were previously assigned to this complex before recent geochronology demonstrated they belonged to the Sleaford Complex and that many units were unrelated. It is thus recommended that the term Lincoln Complex be discontinued. Intruded during the Kimban Orogeny. Previously also included the Donington Suite, Colbert Granite, Moody Suite, Wertigo Granite, Middlecamp Granite, Carappee Granite,  Tournefort Dykes and Coolanie Gneiss.|c. 1850-1690 Ma|||Intrudes the Sleaford Complex.||05-APR-23
28681|Lincoln Complex|71862|5|Briefly described|p1-p2|Paleoproterozoic|Paleoproterozoic|Originally defined by Thomson (1980) to describe the igneous rocks intruding the Archean to Paleoproterozoic Sleaford Complex and Hutchison Group of the Eyre Peninsula. This unit is now obsolete as recent U-Pb geochronology shows that it group together units which aren't genetically related. Originally included the Donington Suite, Colbert Granite, Moody Suite, Wertigo Granite, Middle Camp Granite, Carappee Granite, Minbrie Gneiss, Carpa Granite, Tournefort Dykes and Coolanie Gneiss (Parker, 1993).|c. 1850-1690 Ma|||||18-APR-23
28681|Lincoln Complex|71895|6|Mentioned|APP4. p4, |||||||||
28681|Lincoln Complex|72459|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Lincoln/Cleve domains of the Gawler Craton. Delineated in geophysics by ellipsoid anomalies of varying magnetic strength.||||||
28681|Lincoln Complex|73104|6|Mentioned|p25|||(Blissett et al. 1988). Used to describe predominantly deformed granitoid rocks considered to be Palaeoproterozoic [Paleoproterozoic] in age. Subsequent geochronological studies revealed that it comprises multiple igneous and metamorphic events spanning the Mesoarchaean to Palaeoproterozoic, and the term has been discontinued (Cowley et al. 2017). Originally included the granodiorite later called Nummee Granodiorite.||||||
28681|Lincoln Complex|74367|6|Mentioned|p4|Statherian|Statherian|Kimban Orogeny.|1790-1710 Ma|||||
68700|Lincoln Complex granitoid|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
38534|Lincoln Complex granitoids|23805|6|Mentioned|p4|||Formal name not intended - see Lincoln Complex.  Intruded by the Hiltaba Suite granitoids.  Geological Province: Gawler Craton.||||||
38534|Lincoln Complex granitoids|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
37183|Lincoln Complex""|23719|6|Mentioned|p17|||In the Gawler Craton||||||24-JUN-09
80385|Lincoln Gap Flagstones|71242|14|Not recorded|p9|||Equivalent of the Tent Hill Series.||Of Corunna Group.||||07-FEB-18
29883|Lincoln Gneisses""|43052|6|Mentioned|p74|||Refers to Tilley (1921).||||||
81704|Lincoln Member''|71129|4|Described|p108-110|Neoproterozoic|Neoproterozoic|Of Stuart Shelf. Lower of two informally named units used in the past by Australian Selection Pty Ltd, (1979). Reflects decreasing grain size and carbonate content in upward directions, interpreted to be deposited during transgressive phase in increasingly quieter and deeper waters.||Old informal unit of Tapley Hill Formation.||Lower unit of Tapley Hill Formation. Overlain by Tassie Member. Correlable to Woocalla Dolomite Member or Tindelpina Shale Member.|Laminated dolomitic siltstones and shales with intercalated dolomite laminae and layers; dolomite content increases upwards, and common laminated to ripple cross-laminated sandstone layers.|22-NOV-19
39218|Lincoln complex granite|23731|6|Mentioned|p28|Paleoproterozoic|Paleoproterozoic|Informal.||||||07-NOV-08
81672|Lincoln member''|70334|4|Described|p20,38,48-49|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Stuart Shelf. Informal term used by exploration companies on the Stuart Shelf (Mason 1979). Thickness: up to 140m. Nearshore facies.||Unit of Tapley Hill Formation.||Overlain by Tassie member. Equivalent to Tindelpina Shale Member.|Well laminated dolomitic siltstone and shale containing thin dolomite.|
81687|Little Broken Hill Gabbro''|63102|5|Briefly described|p46|Tonian|Tonian|Of Adelaide Geosyncline. Represents early stages of extensional rifting of Adelaide Geosyncline.|c. 827 Ma|||||
78473|Little Pinbong Rockhole gneisses|65922|5|Briefly described|p31|Statherian|Statherian|Age of ~1670 Ma given. Intruded by St Peter Suite. ||||||
34199|Local Pebble Conglomerate|22645|6|Mentioned|Fig4 p204||Proterozoic|Shown in cross-section of Olympic Dam deposit. Underlies Late Proterozoic Tregolana Shale. Overlies Middle Proterozoic breccias.||||||23-AUG-18
78692|Long Gully member|67721|6|Mentioned|p39 Fig.9|||||Now of the Cook Gap Schist?||||12-MAR-14
81040|Long Ridge Granite|70803|6|Mentioned|p6|||Near Sedan.||||||18-JUN-19
81385|Loogana Sandstone|70397|5|Briefly described|p3|Cretaceous|Cretaceous|Bight Basin. [Likely misspelt; should be Loongana Sandstone].||||Overlain by Madura Formation.||
78429|Loongara Sandstone|65194|6|Mentioned|p31|||High groundwater salinity.||||||
26703|Loveday Soil""|38604|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
26703|Loveday Soil""|41551|6|Mentioned|p464|||||||||
29884|Lower Albite Formation""|43052|5|Briefly described|p84|||||||||
35564|Lower Albite"|23248|6|Mentioned|p170|||||||||
25180|Lower Calana Beds|32823|6|Mentioned|p361|||Misspelling of Callanna||||||
28694|Lower Callana Beds|31797|6|Mentioned|Fig. 2|||Adel.||||||
28694|Lower Callana Beds|32724|6|Mentioned|Fig.1|||Willouran. Correlation||||||
28694|Lower Callana Beds|36083|6|Mentioned|p472|||||||||
28694|Lower Callana Beds|37238|6|Mentioned|Table 1|||||||||
27470|Lower Callanna Beds|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
27470|Lower Callanna Beds|24176|3|Fully described|p9|Adelaidean|Adelaidean|Informal name - see Callanna Beds.  Age is Willouran.  Geological Province: Mount Painter Province.||||||
27470|Lower Callanna Beds|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27470|Lower Callanna Beds|30261|6|Mentioned|Table 1|||Willouran age.||||||
27470|Lower Callanna Beds|30801|6|Mentioned|p5|||Willouran. Table P5-6||||||
27470|Lower Callanna Beds|32720|6|Mentioned|Table 1|||||||||
27470|Lower Callanna Beds|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
27470|Lower Callanna Beds|33468|6|Mentioned|p209|||||||||
27470|Lower Callanna Beds|34535|3|Fully described|p50|||Adelaidean. Willouran. Fig.16||||||
27470|Lower Callanna Beds|34537|6|Mentioned|Fig.9|||||||||
27470|Lower Callanna Beds|34812|6|Mentioned|p111|||||||||
27470|Lower Callanna Beds|35255|6|Mentioned|Fig.6|||||||||
34229|Lower Fitton Formation|22631|6|Mentioned|p177|||||||||
26704|Lower Gawler Range Volcanics|23481|5|Briefly described|p19 Fig 1|||Informal. Geological Province: Gawler Craton.||||||
26704|Lower Gawler Range Volcanics|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Informal.  Geological Province: Gawler Craton.||||||
26704|Lower Gawler Range Volcanics|24346|5|Briefly described|p98 Fig. 1, p101 Fig. 2|Mesoproterozoic|Mesoproterozoic|Informal - see Gawler Range Volcanics.||||||
26704|Lower Gawler Range Volcanics|24597|5|Briefly described|p526 Fig. 1|Mesoproterozoic|Mesoproterozoic|Informal - see Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
26704|Lower Gawler Range Volcanics|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26704|Lower Gawler Range Volcanics|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Informal. Younger succession includes Nonning Rhyodacite and Eucarro Dacite: acid volcanics. Older succession includes Roopena Volcanics: acid and basic volcanics.||||||26-MAY-05
26704|Lower Gawler Range Volcanics|65376|6|Mentioned|p8 Fig.1.1. |Mesoproterozoic|Mesoproterozoic|Name replaced by Gawler Range Volcanics.||||||
26704|Lower Gawler Range Volcanics|65485|6|Mentioned|Fig 1|Mesoproterozoic|Mesoproterozoic|||||||
80331|Lower Janjukian Member|70660|6|Mentioned|p20 fig 11a, p21|||[Mis-spelling of the Lower Janjukian Stage?]||Of Port Willungga Formation||||05-FEB-18
34112|Lower Mannum Formation|22626|6|Mentioned|446 fig 10 447|Early Miocene|Late Oligocene|Geol province Murray Basin. Overlying unit Upper Mannum Formation, underlying unit Ettrick Formation||||||
34110|Lower Morgan Limestone|22626|6|Mentioned|446 fig 10|Middle Miocene|Middle Miocene|Geol province Murray Basin. Overlying unit Upper Cadell Marl, underlying unit Finnis Clay||||||
33864|Loxton-Parilla Sands|10010|5|Briefly described|p17|Pliocene|Late Miocene|Combined term of Brown and Stephenson (1991). Conformable on Bookpurnong beds or disconformable on Renmark Group or Geera Clay; disconformable below Blanchetown Clay.  Average thickness: 30m.Geol.Prov: Murray Basin.Very fine to coarse, gravelly in places.||||||13-AUG-07
33864|Loxton-Parilla Sands|22531|4|Described|p20|Pliocene|Late Miocene|||||||
33864|Loxton-Parilla Sands|22799|3|Fully described|p35|||||||||
33864|Loxton-Parilla Sands|22835|6|Mentioned|P14||Pliocene|||||||
33864|Loxton-Parilla Sands|22857|5|Briefly described|p353 Fig. 24.9|Pliocene|Pliocene|See also Loxton-Parilla Sand. ||||||
33864|Loxton-Parilla Sands|23884|6|Mentioned|p153|||Geological Province: Murray Basin.||||||28-APR-05
33864|Loxton-Parilla Sands|23921|4|Described|p1109, p1114|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
33864|Loxton-Parilla Sands|24103|5|Briefly described|p139 Fig.3|Pliocene|Pliocene|Geological Province: Murray Basin. Age: 6.6-3.5 Ma.||||||
33864|Loxton-Parilla Sands|24439|6|Mentioned|p39 Fig. 21|||||||||06-APR-05
33864|Loxton-Parilla Sands|24440|5|Briefly described|Map legend|||Shallow marine sands.||||||
33864|Loxton-Parilla Sands|60421|5|Briefly described|p407, 408 Fig. 1, 415, 418 Fig. 5|Pliocene|Late Miocene|Geological Province: Murray Basin. Forms strandlines. Overlies: Glenelg River Metamorphic Complex.||||||
33864|Loxton-Parilla Sands|61155|5|Briefly described|p5, p18|Early Pliocene|Late Miocene|Strand plain and fluvial sand deposits. Overlie Bookpurnong beds; overlain by Blanchetown Clay, and by Norwest Bend Formation in the west. Age: ~6.0-2.5Ma. Max. thickness: 150m. Geological Province: Murray Basin.||||||
33864|Loxton-Parilla Sands|61207|5|Briefly described|p281|Pliocene|Late Miocene|See also Loxton-Parilla Sand.  This is a shoreface, beach and possibly alluvial succession of sands and some gravels (Firman 1966; Roy et al 2000). Overlain by Blanchetown Clay.||||||
33864|Loxton-Parilla Sands|61624|6|Mentioned|p471|||Geological Province: Murray Basin.||||||07-APR-09
33864|Loxton-Parilla Sands|63887|5|Briefly described|p20, p21, p22, p21 Fig. 1, p23 Fig. 2|Pleistocene|Late Miocene|Prograding beach strandplains and barrier islands.||||||
33864|Loxton-Parilla Sands|63893|5|Briefly described|p191, p185, p184, p188 Fig. 3|Late Pliocene|Late Miocene|Series of shallow-marine beach, estaurine and fluvial sands. Thick strata, often almost pure quartz. Intermittent heavy minerals. Age: Victorian sequences 3.5 Ma mid-Pliocence. With Blanchetown Clay underlie Shepparton Formation. Geol Prov: Murray Basin.||||||
33864|Loxton-Parilla Sands|64961|5|Briefly described|p269 Fig. 9|Late Pliocene|Late Miocene|See also the misspelt Loxton-Parilla Sand.||||||08-APR-09
33864|Loxton-Parilla Sands|64966|5|Briefly described|pp140|Late Miocene|Early Eocene|Geological province: Murray Basin. An extensive system of arcuate strandlines indicating marine transgression.||||||07-FEB-11
33864|Loxton-Parilla Sands|65552|5|Briefly described|p2; p4-17; p22,25,26,27 App.1,4,5,6|Late Pliocene|Early Pliocene|Loxton Sands and Parilla Sand, undifferentiated in central Murray Basin. Hosts silica, heavy sands, bentonite. Contains Wandella Sandstone, Kerang Sand, Tragowel Members. Underlies Blanchetown Clay; overlies Murray Group, Bookpurnong beds, Olney Formation||||||
33864|Loxton-Parilla Sands|65715|5|Briefly described|p15 Tb.8|||Superseded name for Loxton Sand in Victoria.||||||
33864|Loxton-Parilla Sands|65904|5|Briefly described|p244||Pliocene|20-60m thick, widely distributed across Murray Basin. Mainly marine sand sequence; some beach, deltaic, non-marine sediments. 3 marine facies units: fine grained micaceous sediment, coarse sands and occasional gravel, upwards fining beach sand unit. Contains economic heavy-mineral sands.||||||29-APR-11
33864|Loxton-Parilla Sands|66002|6|Mentioned|p13 Tb.9|||Widely used but invalidly named unit equivalent to Loxton Sand in Victoria. ||||||
33864|Loxton-Parilla Sands|66287|3|Fully described|p24,26,27,31-42, Fig 2,4-5,7-14,17|Early Pliocene|Late Miocene|Progradational strandplain in Murray Basin; over 600 individual ridges. Previous age range ~6 Ma - 2.4 Ma, based on sea level curves, palaeomag and age of overlying Blanchetown Clay. This study's age is from Sr/Sr ratios.|Deposited between 7.2 and 4.5 Ma.|||Overlies and interfingers with Bookpurnong Beds.|Marine, estuarine + minor fluvial depositional environments. Heavy mineral deposits associated.|25-FEB-13
33864|Loxton-Parilla Sands|66934|5|Briefly described|Map legend|Pliocene|Pliocene|Near-surface magnetically-susceptible heavy mineral sands that formed along Murrayian Gulf shoreline in arcs 0.4-1 km wide and tens of kilometres long.||Unit in Wunghnu Group.|||Loosely consolidated cross-bedded micaceous sand, grit and silty sand.|
33864|Loxton-Parilla Sands|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|Murray Basin.||||||
33864|Loxton-Parilla Sands|67179|5|Briefly described|p581|Pliocene|Miocene|Informal, superseded by revised Loxton Sand. Compound name was used because marine strata (Loxton Sand) and dune and fluvial strata (Parilla Sands) are often not possible to map separately.||||||
33864|Loxton-Parilla Sands|68140|5|Briefly described|p1699, p1701-1704, p1707, p1708|||See also Loxton-Parilla Formation. Groundwater in this unit is susceptible to contamination from human activities on the surface.||||Overlain by the Shepparton Formation. Underlain by the Murray Group.|Comprises a sequence of marine sands and silts.|09-FEB-18
33864|Loxton-Parilla Sands|69572|6|Mentioned|p1190-1191|Pleistocene|Miocene|Contains fossil koala of Phascolarctos yorkensis.||||||
33864|Loxton-Parilla Sands|70718|5|Briefly described|p90, 104|||Murray Basin. Obsolete name, see the Loxton Sand which has replaced it.||||||30-MAY-19
33864|Loxton-Parilla Sands|72445|5|Briefly described|App.6 p1 Tb.1, p5, p7; App.7 p7.|Pliocene|Late Miocene|Spelt as 'Loxton-Parilla Sand' in App.6 p1 Tb.1. App 6 suggests in Stavely 11, 14 samples, but well log indicates Bookpurnong Formation at these depths. Described App 7 as fluvio-lacustrine, App.6 as shallow marine.|< 5.72 Ma||Probably includes Wandella Sandstone Member.|Shown as overlying Bookpurnong beds and partially and unconformably underlying Blanchetown Clay and partially equivalent to Parilla Sand and Loxton Sands.|Includes sand.|
33864|Loxton-Parilla Sands|73118|5|Briefly described|p12, 17, 21, 24, 30, 34, 37, 45, 48, 53|Pliocene|Miocene|See also p58, 61, 64, 81. Forms blanket of sand beneath almost the entire SW Murray Basin. 100m thick; mainly <60m. CRA Exploration found (between 1980-1992) several world-class mineral sand accumulations along the southern margin region of the Murray Basin. Drill core summary logs. Strand-plain (shallow-marine, beach and estuarine) deposits flanked/overlain by fluvial and fluvio-lacustrine deposits.||||Overlies Grampians Group, Duddo Limestone, Geera Clay, Bookpurnong Beds, Winnambool Formation and Olney Formation. Is overlain by Woorinen and Shepparton Formations, Molineaux-Lowan Sands.|Unconsolidated to weakly cemented,yellow-brown fine to coarse well-sorted quartz sand, sandstone, with minor clay, silt, pebbly conglomerate.|
83137|Loxton-Parilla Sands''|73228|4|Described|p58-59|||Name has been widely used to describe the Pliocene strandline sands of the Murray Basin and was invoked to address difficulties encountered in stratigraphic correlation across state boundaries, particularly between the 'Loxton Sands' of Ludbrook (1957), the 'Parilla Sand' of Firman (1966), and the 'Diapur Sandstone' of Lawrence and Goldberry (1973). Defined as a 'single composite sand sheet' deposited in a complex array of strandplain environments varying from shallow to marginal marine, estuarine and fluvial (Brown and Stephenson, 1991). Fossil poor but contains calcareous, often fossiliferous, facies in the western and southwestern Murray Basin. Well-laminated horizons often exhibit cross-bedding, particularly within the quartz-gravel units. Thickness typically ranges from 20 to 60 m and is up to 150 m in places. Contains large concentrations of heavy minerals (mainly rutile, zircon and ilmenite; Roy et al. 2000).||||Disconformably overlain by upper Norwest Bend Formation.|Fine to coarse, well-sorted quartz sand and sandstone, yellow-brown in colour, with minor silt, clay and pebble conglomerates, locally containing micaceous quartz sands and/or gravel facies and large concentrations of heavy minerals.|
80044|Luxemburg amphibolite|62993|5|Briefly described|p31, 32|Neoproterozoic|Neoproterozoic|Local intrusive amphibolite unit central to the Luxemburg goldfield, Mingary district. .Also described as a 'mafic body', with Delamerain Orogeny fabrics. Temporally equated with Gairdner Dyke Swarm. Considered to be source of gold.|~827 Ma inferred.||||Amphibolite.|19-DEC-21
35832|Luxton Sand|23322|5|Briefly described|957 Fig.2|||Geological Province: Gambier Basin.||||||07-SEP-09
68702|Mabel Creek Ridge-metasediments|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Banded iron formation. Geological Province: Gawler Craton.||||||07-NOV-08
78341|Mackundra Formation|68734|6|Mentioned|p218 Fig.2|||See Mackunda Formation in this paper.||||||16-JAN-17
28706|Macumba Sandstone""|33938|6|Mentioned|p41|||||||||
28706|Macumba Sandstone""|44393|6|Mentioned|p.6|||As unpublished name.||||||
81629|Magazine Clay''|72247|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Intersected in a stratigraphic exploration drillhole (Pacminex EX 62) near White Cliff Dam (Tonkin 1974b, p. 119). Thickness: 9m. Terminology now obsolete; this interval was later identified as deeply weathered Tapley Hill Formation.|||||Kalolinitic siltstone; white kaolinitic clay.|
81630|Magazine Hill Clay''|71129|5|Briefly described|p107|Neoproterozoic|Neoproterozoic|Of Stuart Shelf. Informally named by Mount Gunson Mines Pty Ltd (1975), representing light-coloured, near-surface, deeply weathered, kaolinitic shale facies of the Tapley Hill Formation.||Unit of Tapley Hill Formation.|||Light-coloured, near-surface, deeply weathered, kaolinitic shale facies.|
81630|Magazine Hill Clay''|72247|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Same unit as Magazine Clay. Now Tapley Hill Formation, not Tregolana Shale, as previously thought.||||||16-SEP-19
80277|Main Group Granites|71341|6|Mentioned|p196|Palaeoproterozoic|Palaeoproterozoic|Eastern Aileron Province. [Misspelling of the Main Group granites].|ca. 1771-1747 Ma||||Granites.|06-NOV-17
69045|Malabena Sandstone Member, upper|60712|6|Mentioned|p35|Early Cambrian|Early Cambrian|Informal - see Malabena Sandstone Member.||||||
73970|Malbooma granite""|61556|5|Briefly described|p9-10|Carpentarian|Carpentarian|In Central Province - Mount Christie.||||||
67961|Mambray Formation""|44133|6|Mentioned|p226|||||||||
27475|Mampuwordu Sands|30804|5|Briefly described|p13|||On Table 1||||||
27475|Mampuwordu Sands|30807|6|Mentioned|p101|||Suggested map symbol||||||
27475|Mampuwordu Sands|30919|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
27475|Mampuwordu Sands|32007|6|Mentioned|p158|||||||||
27475|Mampuwordu Sands|33824|6|Mentioned|Table 2|||||||||
27475|Mampuwordu Sands|34308|6|Mentioned|Fig.84|||Pliocene. Cor. chart||||||
27475|Mampuwordu Sands|36213|6|Mentioned|Fig.2|||||||||
27475|Mampuwordu Sands|38068|6|Mentioned|Fig.7|||||||||
27475|Mampuwordu Sands|38982|6|Mentioned|p69|||||||||
27475|Mampuwordu Sands|40755|5|Briefly described|App.3.1|||||||||
27475|Mampuwordu Sands|40756|5|Briefly described|p1|||||||||
27475|Mampuwordu Sands|40757|6|Mentioned|p76|||||||||
27475|Mampuwordu Sands|41537|6|Mentioned|p350|||||||||
27475|Mampuwordu Sands|42375|6|Mentioned|p34|||See also Mampuwordu Member, Table 1.||||||
27475|Mampuwordu Sands|42477|5|Briefly described|p186|||||||||
27475|Mampuwordu Sands|44223|14|Not recorded|p.157,158,159||Pliocene|Fig.2. Palankarinna Fauna.||||||
27475|Mampuwordu Sands|44228|14|Not recorded|p.129,131||Pliocene|||||||
27475|Mampuwordu Sands|44238|14|Not recorded|Fig.3||Pliocene|||||||
27475|Mampuwordu Sands|45128|6|Mentioned|p56|||||||||
42512|Mampuwordu Sandstone|23818|5|Briefly described|p174 Fig.84|Pliocene|Pliocene|Geological Province: Great Artesian Basin.||||||
73762|Mannum Formation, lower|63460|5|Briefly described|p839 Fig.2b||Late Oligocene|Informal - see Mannum Formation. Lower/upper Mannum boundary aproximates the Oligo-Miocene boundary. Geological province: Murray Basin.||||||
73763|Mannum Formation, upper|63460|5|Briefly described|p839 Fig.2b|Early Miocene|Early Miocene|Informal - see Mannum Formation. Includes the Swan Reach Dolomite Member. Max. thickness: 42m.  Lower/upper Mannum boundary aproximates the Oligo-Miocene boundary. Geological province: Murray Basin.||||||
68721|Mannum formation|24558|6|Mentioned|p664, p666|Miocene|Miocene|Informal - see Mannum Formation.||||||30-JAN-08
37211|Maralinga Formation|24396|5|Briefly described|p221|Middle Eocene|Middle Eocene|Correlated with lower part of Pidinga Formation.||||||08-FEB-10
37211|Maralinga Formation|24397|3|Fully described|p233|Late Eocene|Middle Eocene|Includes rocks formerly included in lower Pidinga Fm., Poelpena and Wanilla Fms.  Direct equivalent of the North Royal Formation in Western Australia.  Overlain by Paling Formation.  Geological Province: Eucla Basin.||||||
37211|Maralinga Formation|65194|6|Mentioned|p170|||Early palaeovalley deposits in Gawler Craton.||||||
80386|Marino Group""|71242|14|Not recorded|p11|||||||||
25208|Marinoan "Series"|37627|6|Mentioned|p188|||||||||
28724|Marinoan Formation|39558|6|Mentioned|Table 2|||||||||
34817|Marinoan glacials|22911|6|Mentioned|37||Neoproterozoic|Marinoan age, glacial origin sediments, not a stratigraphic name.||||||
73187|Marla Group, upper|63224|6|Mentioned|p9|Cambrian|Cambrian|Informal - see Marla Group. Geological Province: Amadeus Basin.||||||07-FEB-08
35700|Marla Sequence""|23282|6|Mentioned|p68|||Term introduced by Krieg (1973) and superced by Marla Group (Benbow 1982).||||||
42112|Marne River Volcanics""|60567|6|Mentioned|p37|||Informal - see Marne River Volcanics.||||||
26724|Marree Sub-Group|42375|5|Briefly described|p133|Cretaceous||Misspelling of Marree Subgroup?||||||
26724|Marree Sub-Group|65194|6|Mentioned|p46|||[Formal name is Marree Subgroup]. Includes Bulldog Shale.||||||
25212|Marrimelia Formation|29721|6|Mentioned|p141|||||||||
28730|Maslin Sand""|35689|6|Mentioned|p12|||||||||
38732|Maslin Sand, upper|24397|5|Briefly described|p234 Tb. 2|||Informal name.||||||
68924|Massena Bay Gneisses|61070|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Sleaford Complex. Banded quartz-feldspar-biotite +/- garnet gneiss, minor calcsilicate gneiss, abundant quartzofeldspathic orthogneiss. Geological Province: Gawler Craton.||||||12-JAN-10
68924|Massena Bay Gneisses|61307|6|Mentioned|p37|||Migmatitic quartzo-feldspathic orhtogneissic xenoliths found in the Lincoln Batholith. See also Massena Bay Gneiss. ||||||
25215|Massena Bay mylonite|41972|5|Briefly described|p397|||||||||
41688|Massena Bay orthogneiss|50605|6|Mentioned|p3.1|||||||||
35695|Maurice Group|23282|6|Mentioned|p56|||of Zanedg (1995). Superced by Lake Maurice Group.||||||
35695|Maurice Group|63397|2|Defined|26|Neoproterozoic III|Neoproterozoic III|Mainly siliciclastics and minor silty limestone. Max. thickness: 2000m. Unconformably overlies: Alinya Formation.  Overlain by: Dey Dey Mudstone. Type section in text.||||||
35695|Maurice Group|69648|6|Mentioned|p18|||Of Zang (1995). Renamed Lake Maurice Group by Morton (1997).||||||
74090|McFadden Formation equivalent""|61732|6|Mentioned|p89|||Name now abandoned and replaced by Lungkarta Formation. Cannot be equated with the McFadden Formation.||||||07-FEB-11
68842|McKinlay Formation|61015|6|Mentioned|p46|||Oil recovered from this unit.||||||
29674|McKinlay beds|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
81705|McLeay Beds''|71129|5|Briefly described|p101,107|Tonian|Tonian|Of Stuart Shelf. Nomenclature of Gersteling and Heape (1975). Similar stratigraphic position to Elizabeth Creek Conglomerate and Moonlight Conglomerate. Interpreted to be Sturtian (early Neoproterozoic) in age, and possibly either a basal unit of Tapley Hill Formation (Thomson et al., 1976), or more recently interpreted to be part of Backy Point Formation (Mason et al., 1978, Cowley, 1991a).||||Partial equivalent to Backy Point Formation.||
81631|McLeay beds''|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Woomera area. Of Adelaide Geosyncline.||||Overlain by Gunson beds. Underlain unconformably by Pandurra Formation. Transitional to Tapley Hill Formation.||16-SEP-19
81631|McLeay beds''|73227|6|Mentioned|p36|||[Written as 'McLeay beds']. Of Maiden (1974) in reference to discontinuous beds in the McLeay Siding-Ironstone Lagoon-Manganese Workings locality overlying the Pandurra Formation.||||||
70177|Meena Mudstone Member|61732|5|Briefly described|p58 Fig. 22|Ediacaran|Ediacaran|Misspelt in figure perhaps? Of the Narana Formation (Ungoolya Group). Geological Province: Officer Basin.See also Mena Mudstone Member of the Narana Formation.||||||07-FEB-11
35699|Mena Mudstone|23282|6|Mentioned|p67|||Of Sukanta (1993).  Superseded by Mena Mudstone Member.||||||28-MAR-06
29843|Meningie Well Formation|22884|2|Defined|p40 Fig. 1, p45||Paleoproterozoic|Of Broken Hill Group. Contains Bimba Sulphide Member. Overlain by Mount Howden Formation; underlain by Peryhumuck Formation. Max. thickness: 500m.Correlated to Weekeroo Formation. Thin units+lenses of calc-silicate, calc-albitite, marble, sulphidic ironst||||||26-MAR-09
29843|Meningie Well Formation|63102|6|Mentioned|p33|||Geological province: Broken Hill Domain, Curnamona Province. Nomenclature of Laing (1996b). Now considered to be part of Oonatra Creek Formation.||||||
29843|Meningie Well Formation|70657|6|Mentioned|p40|||Laing (1996). The type area is in the Meningie Well - Mulga Bore Creek area.||||||
22313|Meramangye beds|23282|6|Mentioned|p57|||of Stainton et al (1988). Superseded Meramangye Formation.||||||17-FEB-15
81881|Merinjina Diamictite|72613|6|Mentioned|p3|Cryogenian|Cryogenian |Shown as Sturtian age. Northern Flinders Ranges. See also the Merinjina Tillite. Last glacial deposits of Sturtian glaciation.|tuff near top dated at 663+/- 0.11 Ma|Of Umberatana Group.||||
78872|Merirjina Tillite|62903|6|Mentioned|p729|||[Misspelling of Merinjina Tillite (Yudnamutana Subgroup, Adelaide Rift Complex)]. Merinjina Tillite occurs in Sturtian glaciation (Preiss et al. 1998) that correlates with Areyonga Formation. Presented in text as Sturt-Appila-Pualco-Bolla Bollana-Merirjina Tillites.||Yudnamutana Subgroup||Sturtian glacial units overlain by Tapley Hill Formation||
77083|Mern Merna Formation|62592|5|Briefly described|p50 Table 5.1.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Hawker Group.||Overlies Wilkawillina Limestone. Is overlain by Oraparinna Shale.|Deep-water limestone.|
67964|Mernmerna Formation, lower|44133|5|Briefly described|p23|||Conformably overlies: Wirrapowie Limestone. Maximum Thickness: 650m.||||||
67964|Mernmerna Formation, lower|60889|4|Described|p247 Fig.4|Early Cambrian|Early Cambrian|North-Central Trough, Arrowie Basin.||Hawker Group||Overlies Wirrapowie Limestone. ?Encloses Midwerta Shale.||
67964|Mernmerna Formation, lower|71102|6|Mentioned|p247,249|Series 2|Series 2|Of Arrowie Basin. Intersected sections: BHG (Bullock Head Gap, SW Arrowie Syncline), LMNB (Lower Mernmerna, North Boundary Creek, Chambers Gorge, E Flinders Ranges).||||||
67965|Mernmerna Formation, middle|44133|6|Mentioned|p24|||||||||
67966|Mernmerna Formation, upper|44133|5|Briefly described|p25, 26|||Maximum Thickness: 700m. Conformably overlies: Bunkers Sandstone. Intertounges with Oraparinna Shale.||||||
67966|Mernmerna Formation, upper|60889|4|Described|p247 Fig.4, p249, p252 Fig.11|Early Cambrian|Early Cambrian|Is main transgressive unit beyond shelf edge. Thickness: ~2 500 m. North-Central Trough, Arrowie Basin. Shown as upper Mernmerna Formation.||Hawker Group||Encloses Nepabunna Siltstone.|Generally a dark silty limestone.|
67966|Mernmerna Formation, upper|71102|5|Briefly described|p244,246-246,251,253-254,267,269|Series 2|Series 2|Of Arrowie Basin. Typical dark, flaggy, micritic limestones with gradually increasing siliciclastic input. Intersected sections: DBS (Donkey Bore Syncline), 10MS (10 Mile South, Bunkers Graben), BHG (Bullock Head Gap, SW Arrowie Syncline).||||||
75062|Mernmerna Limestone|64829|5|Briefly described|p1084 Fig. 1|Early Cambrian|Early Cambrian|||||||07-FEB-11
75062|Mernmerna Limestone|65313|6|Mentioned|p576 Fig. 5|Cambrian|Cambrian|||||||
83057|Merrimellia Formation|73244|6|Mentioned|p86|Permian|Permian|[Possibly a misspelling of Merrimelia Formation]. Cooper Basin. Glacial. Oil and gas.||||||
83057|Merrimellia Formation|73343|6|Mentioned|p337|Permian|Permian|Cooper Basin. Hosts oil and gas. [Probably a misspelling of Merrimelia Formation].||||Overlain by Tirrawarra Formation.||
83057|Merrimellia Formation|73479|5|Briefly described|p156 Fig.2, p160|Permian|Permian|Cooper Basin. Glacial depositional environment. [Misspelling of Merrimelia Formation?]||||Underlies Tirrawarra Formation||
29889|Mica Schist""|43052|6|Mentioned|p87|||||||||
69768|Michael Hills layered intrusion|61339|6|Mentioned|Map legend|||Informal name.||||||
29443|Middle Murravian Series""|42966|6|Mentioned|p149|||refers to Tate (1885)||||||
28752|Middleback Group""|37461|5|Briefly described|p317|||||||||
81108|Middleback Iron Formation, Lower|72058|5|Briefly described|p172|||Middleback Ranges, Gawler Craton. Min depositional age ~2.56 Ga from overlying Cook Gap Schist.||Middleback Group||Overlies the Katunga Dolomite. Overlain by the Cook Gap Schist.||18-JUN-19
81108|Middleback Iron Formation, Lower|72484|5|Briefly described|p2-3|||Eyre Peninsula, Gawler Craton. Hosts the predominant part of the iron deposits in the Middleback Ranges.|>2565 Ma (MDA: Szpunar et al., 2011).|Middleback Subgroup.||Gradationally overlies Katunga Dolomite. Is overlain gradationally by Cook Gap Schist.||
81109|Middleback Iron Formation, Upper|72058|5|Briefly described|p172|||Middleback Ranges, Gawler Craton. This unit has been suggested to be a potential structural repition of the Lower Middleback Iron Formation.||Middleback Group||Overlies the Cook Gap Schist (age ~2.56 Ga).||18-JUN-19
81109|Middleback Iron Formation, Upper|72484|6|Mentioned|p2|||||Middleback Subgroup.||Gradationally overlies Cook Gap Schist.||
68925|Middleback Jaspilite, Lower|23731|5|Briefly described|p20, p28, p72|||Informal. Overlies Katunga Dolomite.||||||
68925|Middleback Jaspilite, Lower|41667|6|Mentioned|p5|||||||||
68925|Middleback Jaspilite, Lower|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Middleback Subgroup. Fine-grained quartzite, haematitic quartzite; locally cherty and graphitic. Minor graphitic fine grained schist. Overlies Katunga Dolomite. Underlies Cook Gap Schist. Geological Province: Gawler Craton.||||||12-JAN-10
68925|Middleback Jaspilite, Lower|61307|6|Mentioned|p61 Fig. 27|||Informal name.||||||
68925|Middleback Jaspilite, Lower|62893|4|Described|Map Legend, p10, p25, p37|Early Proterozoic|Early Proterozoic|Reflects marine chemical sedimentation. Silicate-facies iron formation consisting of recrystallised and graphitic chert with low iron content. Grunerite commonly occurs with the iron oxide. Expressed as long, linear, northeast to north-trending anomalies in aeromagnetic datasets.||Middleback Subgroup, Hutchison Group||Underlain by and interfingers with Katunga Dolomite. Underlain by Warrow Quartzite. Overlain and interlayered with Cook Gap Schist.|Quartz-veined grunerite schist, banded diopside-amphibole quartzite with variable magnetite content, and graphitic quartzite.|
68925|Middleback Jaspilite, Lower|68131|5|Briefly described|p57-58|Paleoproterozoic|Paleoproterozoic|Parker and Lemon (1982). Eastern Eyre Peninsula. Occasionally mis-spelt as Lower Middleback Jaspelite. Contains South Australia's most productive iron ore deposits.||Middleback Subgroup.|||Includes banded iron formations.|
68925|Middleback Jaspilite, Lower|71235|6|Mentioned|p9|||||Hutchison Group||||
68925|Middleback Jaspilite, Lower|71536|5|Briefly described|p79-80, p88|||Wilgerup sequence. Mistakenly referred to as the Lower Middleback Formation on p88.||||Conformably (transitionally) overlies the Katunga Dolomite. Overlain by the Cook Gap Schist.|Hematite BIFs, hematite clays, magnetite-hematite BIFs, massive hematites and cherts.|
68925|Middleback Jaspilite, Lower|71859|6|Mentioned|p18|||||Hutchison Group||||
68925|Middleback Jaspilite, Lower|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Haematite, banded, with quartzite + magnetite, carbonate, schist and chert. Grades into jaspilite in places.|
68926|Middleback Jaspilite, Upper|35298|6|Mentioned|p946|||||||||
68926|Middleback Jaspilite, Upper|41667|6|Mentioned|p5|||||||||
68926|Middleback Jaspilite, Upper|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Middleback Subgroup. Magnetite-hornblende-grunerite quartzite, quartzite, minor epidote. Interbanded with Burrawing Amphibolite. Contacts with Cook Gap Schist and Burrawing Amphibolite commonly gradational. Geological Province: Gawler Craton.||||||12-JAN-10
68926|Middleback Jaspilite, Upper|61307|6|Mentioned|p61 Fig. 27|||Informal name.||||||
68926|Middleback Jaspilite, Upper|62893|4|Described|Map Legend, p. 10-12, 22, 25,28,36-38,40|Early Proterozoic|Early Proterozoic|Locally known as Mount Shannan Iron Formation. Reflects a period of marine transgression and chemical sedimentation. Five principal rock types of this unit were described by Rankin and Flint (1987) from the Broad View 1 drillhole [see article]. Has significantly lower iron content in the Kimba mapsheet area compared to the Middleback Ranges. Expressed as long, linear, northeast to north-trending anomalies in aeromagnetic datasets. May be synchronous with acid volcanics of the Bosanquet Formation.||Middleback Subgroup, Hutchison Group||Conformably underlain by Cook Gap Schist.|Massive, poorly banded, reddish pink to grey dolomite with crenulated mica schist and occasional tremolite-rich layers grading upwards to interlayered pink to white, cherty, grey to red jaspilitic quartzite and medium to fine-grained dolomite.|
68926|Middleback Jaspilite, Upper|68131|5|Briefly described|p57-58|Paleoproterozoic|Paleoproterozoic|Parker and Lemon (1982). Eastern Eyre Peninsula. Occasionally mis-spelt as Upper Middleback Jaspelite.||Middleback Subgroup.|||Includes banded iron formations.|
68926|Middleback Jaspilite, Upper|71235|6|Mentioned|p9|||||Hutchison Group||||
68926|Middleback Jaspilite, Upper|71536|5|Briefly described|p79-80|||Wilgerup sequence.||||Overlies the Lower Middleback Jaspilite.|Hematite BIFs, hematite clays, magnetite-hematite BIFs, massive hematites and cherts.|
68926|Middleback Jaspilite, Upper|71859|6|Mentioned|p18|||||Hutchison Group||||
68926|Middleback Jaspilite, Upper|73103|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Jaspilite.|
75993|Middleback Jaspilite, lower|65379|5|Briefly described|p642|Paleoproterozoic|Paleoproterozoic|Overlies Katunga Dolomite with complex contact, generally marked by recrystallised chert beds alternating with dolomite.||||||
69794|Middleback Quartzite, Lower|30806|6|Mentioned|p949|||||||||
69794|Middleback Quartzite, Lower|31203|6|Mentioned|p22|||||||||
69794|Middleback Quartzite, Lower|35298|6|Mentioned|p946|||||||||
73967|Middleback Quartzite, Upper|30806|6|Mentioned|p946|||||||||
73967|Middleback Quartzite, Upper|61556|6|Mentioned|p8|||Name probably invalid or obsolete? May be equated with Greenpatch Metajaspilite.||||||21-NOV-07
36997|Middleback Subgroup, Lower|23492|6|Mentioned|p6|||Informal name.||||||
41689|Middleback subgroup|50605|5|Briefly described|p3.3, 8.7|||Of the Hutchison Group. Geological Province: Gawler Craton and Curnamona Province.||||||22-JUN-09
41689|Middleback subgroup|72459|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Lincoln/Cleve domains of the Gawler Craton. Banded iron formations display high, linear anomalies.|||||Banded iron formations.|
34342|Middlecamp Granite|22629|6|Mentioned|fig2p147|Statherian|Statherian|Age: 1730Ma.||||||18-JAN-07
34342|Middlecamp Granite|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34342|Middlecamp Granite|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Lincoln Complex. Age: 1753-1738Ma. Syntectonic adamellite to granodiorite.||||||07-NOV-08
34342|Middlecamp Granite|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Syntectonic adamellite to granodiorite. Age: 1753-1738 Ma.||||||07-NOV-08
34342|Middlecamp Granite|63020|5|Briefly described|p983, p987|Paleoproterozoic|Paleoproterozoic|See also Middle Camp Granite. Age: 1730Ma. Geological Province: Gawler Craton.||||||07-NOV-08
34342|Middlecamp Granite|63866|5|Briefly described|p6, p9, p19, p31|||Cleve Domain, Gawler Craton.|c. 1740-1730 Ma (Fanning et al., 2007)|Donington Suite||||
34342|Middlecamp Granite|64576|6|Mentioned|p625 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: c. 1730Ma.||||||
34342|Middlecamp Granite|65376|6|Mentioned|p38.|Paleoproterozoic|Paleoproterozoic|See Middle Camp Granite.||||||
34342|Middlecamp Granite|65772|6|Mentioned|p229 Fig.2|Statherian|Statherian|~1730 Ma||||||
34342|Middlecamp Granite|66302|5|Briefly described|p18, p26, p65|Statherian|Statherian|Intruded during the Kimban Orogeny. Ages are from Fanning et al. (2007). Another age of 1736 +/- 6 Ma has been provided from Fraser and Neumann (2007).|1737 +/- 7 Ma to 1726 +/- 7 Ma ||||Grey, medium-grained, foliated granite of monzogranite to granodioritic composition that is intruded by pegmatite dykes.|
34342|Middlecamp Granite|67536|6|Mentioned|Map Legend|Statherian|Statherian|Gawler Craton. Of Kimban Orogeny.|1731 +/- 7 Ma||||Granite.|
34342|Middlecamp Granite|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic|Associated with the Kimban Orogeny. Mapped with Donington and Moody Suites as a single unit.||||||
34342|Middlecamp Granite|70382|6|Mentioned|p32|Statherian|Statherian|Geological province: Gawler Craton. Informal name used by Fanning, Reid and Teale 2007 to describe a granite from the southern Gawler Craton. Possible source for some of Quartoo Sand Member inherited zircon.|~1730 Ma|||||
34342|Middlecamp Granite|71317|6|Mentioned|p15|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.||||||
34342|Middlecamp Granite|71318|5|Briefly described|p3,37-38,40|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017968 (granite) yielded an interpreted (upper intercept age) best estimate of magmatic crystallisation age of 1742+\-43 Ma, with inherited zircon compotents at c. 2500-2440 Ma. Zircon characteristics, petrography, U-Pb isotopic results and geochronological interpretation are provided.|||||Granite.|10-DEC-19
34342|Middlecamp Granite|72462|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Gawler Craton.||||||
34342|Middlecamp Granite|73525|6|Mentioned|p20|Statherian|Statherian|Gawler Craton, eastern. Cleve Domain. See also Middle Camp Granite.|1745-1725 Ma|||||
39571|Middleton Formation|24465|6|Mentioned|p358|||Misspelt - see Middleton Sandstone.||||||
79408|Milendella Limestone|70407|5|Briefly described|p113||Cambrian|Incised valleys associated with this unit.||Of Kanmantoo Group.||||
27669|Milendella Limestone Member|22643|5|Briefly described|p196, fig6|Early Cambrian|Early Cambrian|Within Blowhole Creek Siltstone Member. Age: Botomian.||||||
27669|Milendella Limestone Member|22840|6|Mentioned|P38|||||||||
27669|Milendella Limestone Member|24465|6|Mentioned|p347|Early Cambrian|Early Cambrian|Superseded by Milendella Member.||||||
27669|Milendella Limestone Member|30051|6|Mentioned|Fig.1|||Middle Cambrian age.||||||
27669|Milendella Limestone Member|30801|6|Mentioned|p5|||Strangway Hill Formation. Table P5-6||||||
27669|Milendella Limestone Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
27669|Milendella Limestone Member|32439|6|Mentioned|p99|||||||||
27669|Milendella Limestone Member|33471|6|Mentioned|p556|||||||||
27669|Milendella Limestone Member|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
27669|Milendella Limestone Member|41947|2|Defined|p18|Early Cambrian||||||||
27669|Milendella Limestone Member|42243|6|Mentioned|p211|||||||||
27669|Milendella Limestone Member|42270|5|Briefly described|p361|||See also Fig.2||||||
27669|Milendella Limestone Member|42499|5|Briefly described|Map legend|Cambrian||||||||
27669|Milendella Limestone Member|43759|5|Briefly described|p446|||||||||
27669|Milendella Limestone Member|44133|5|Briefly described|p15, 17|||Of the Carrickalinga Head Formation.||||||
27669|Milendella Limestone Member|60712|5|Briefly described|p30 Fig. 3|Early Cambrian|Early Cambrian|Of the Strangway Hill Formation (Kanmantoo Group).  Of Thompson and Horwitz (1962) and Thompson (1969a, 1969b).||||||
27669|Milendella Limestone Member|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of Carrickalinga Head Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||
77780|Miltalie Orthogneiss|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 2000 Ma|||||
77781|Miltalie Paragneiss|67181|5|Briefly described|p616 Fig.1|Paleoproterozoic|Paleoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 2000 Ma|||||
80275|Miltalie gneiss|71341|6|Mentioned|p188 fig 7|||||||||
25239|Minalton Conglomerate|42270|6|Mentioned|p364|||||||||
38344|Minbrie Gneisses|23791|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
75937|Mingary dykes|65369|5|Briefly described|p35, 36|Neoproterozoic|Neoproterozoic|South Australian mafic dykes. Thought to be correlative with the Gairdner Dyke Swarm and Keene Basalt.||||||19-MAR-12
70622|Mingary group|62373|5|Briefly described|p511|||Informal group in the metabasite suite of the Curnamona Province - Lady Louise Suite, Broken Hill Domain.||||||
30612|Minnipa Granite|61556|14|Not recorded|p10|Mesoproterozoic|Mesoproterozoic|||||||23-DEC-16
30612|Minnipa Granite|65390|5|Briefly described|p26 Tb.1|Calymmian|Calymmian|Of Hiltaba Suite. Pinkish, coarse-grained granite-adamellite, minor porphyritic varieties and minor aplite dykes. Aged 1477 +/- 34 Ma (Rb-Sr: Webb et al., 1986).||||||
41691|Minnipa granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Of the Kokatha suite. Age: 1592Ma.||||||07-FEB-11
41691|Minnipa granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
28757|Mintabie Sandstone|23818|6|Mentioned|p115 Fig.48|||||||||
28757|Mintabie Sandstone|31914|6|Mentioned|p98|||Equiv. Wanna Beds?||||||
28757|Mintabie Sandstone|34280|3|Fully described|p10|||See also PP10, 12. Silurian - Devonian ?||||||
28757|Mintabie Sandstone|34612|6|Mentioned|Fig.48|||||||||
28757|Mintabie Sandstone|41276|6|Mentioned|p61|||||||||
28757|Mintabie Sandstone|45149|6|Mentioned|p43|||||||||
28757|Mintabie Sandstone|73090|6|Mentioned|p12 Fig.7|||||||||
28757|Mintabie Sandstone|73203|6|Mentioned|p649-650|||Hosts opal at Mintabie.||||||
35705|Mintabie beds""|23282|6|Mentioned|p83|||Synonym of Blue Hills Sandstone.||||||
39675|Mirikata Formation equivalents|24175|6|Mentioned|p34 Fig. 7|Cenozoic|Cenozoic|Informal name.||||||19-NOV-08
23800|Mirra Formation""|38926|6|Mentioned|p37|||||||||
23800|Mirra Formation""|42238|6|Mentioned|p73|||||||||
68060|Mitalie Gneiss|24526|5|Briefly described|palaeopro|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by Hutchison Group.  Age of its prescursor: 2000+/-13Ma (Fanning 1997).  Geological Province: Gawler Craton.  See also p96 Fig. 2.||||||07-NOV-08
68060|Mitalie Gneiss|64313|6|Mentioned|p450|Paleoproterozoic|Paleoproterozoic|Age: ca.2000Ma. Geological province: Gawler Craton. See also Fig. 1,  and p451 Figs.2a,b.||||||09-FEB-10
68060|Mitalie Gneiss|71037|5|Briefly described|p21 Fig.1|Paleoproterozoic|Paleoproterozoic|Shown only on 'Outcropping geology and mineral deposits of northern Eyre Peninsula' map p21 Fig.1.||||Shown as older than Donington Suite.|Gneiss.|
68060|Mitalie Gneiss|71348|6|Mentioned|p201|Orosirian|Orosirian|Geological province: Gawler Craton.|c. 2000 Ma|||||
80467|Mitcham Slates and Quartzites""|71529|14|Not recorded|p1|||Replaced by Belair "group"?||||||
41550|Mitcham quartzite|50615|6|Mentioned|p303, Fig. 2.|||Informal. Of the Belair Subgroup Formation. Geological Province: Adelaide Fold Belt.||||||
29456|Molineaux Formation|42966|6|Mentioned|p266|||||||||
34522|Molineaux Sand""|22799|6|Mentioned|p46|||Molineaux-Lowan Sands in NSW.||||||
28762|Molyneux Sand|32859|5|Briefly described|p69|||Recent||||||
80627|Mona Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton.|ca 1775 Ma|Wallaroo Group||Overlain by the Matta Formation.|Silicic volcanics, porphyry.|
22362|Mona Volcanics|73026|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|Northern Yorke Peninsula.|1740 +/- 6 Ma|Wallaroo Group||||
22362|Mona Volcanics|73027|6|Mentioned|p7|Statherian|Statherian||1740 +/- 6 Ma (Fanning et al, 2007)|Wallaroo Group||||
27490|Montacute Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
83691|Monteith Granite|73430|6|Mentioned|p495|Middle Ordovician|Early Ordovician|A-type granite. Also written as the granite at Monteith (sample KW08-15).|470.1+/-1 Ma LA-ICP-MS zircon U-Pb|Padthaway Ridge suite|||Granite.|
77084|Montstephen Metabasalt|62592|5|Briefly described|p15. |||Olary Domain. Minor mafic volcanism synchronous with the Basso Suite volcanics and intrusives.||||||
77084|Montstephen Metabasalt|63102|4|Described|p14,30-31,34,38-40,44,47,49|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. Formerly informally known as Weekeroo amphibolite (Forbes 1991). Comprises several metamorphosed mafic bodies intercalated with a metasedimentary sequence, but showing variation between the Morialpa, Coppertop and Walparuta inliers. Shows evidence of hydrothermal brecciation, on the northern margin of Montstephen Metabasalt in the Coppertop and Walparuta inliers. Stratigraphically located either in lower Ethiudna Subgroup, or high up in upper part of Wiperaminga Subgroup.||||Coeval with Basso Suite and Ethiudna Subgroup deposition.|Mafic extrusives (pillows and amygaloidal textures), dykes and sills.|
77084|Montstephen Metabasalt|63866|5|Briefly described|p41|||Similar in age to the Poodla Hill Granodiorite [an exact age is not provided]. Could be included in the Basso Suite.||||||
77084|Montstephen Metabasalt|70657|4|Described|p14, p16, p29-31, p41, p45-46, p50-51|Statherian|Statherian|See also p54-55, p61, p66. Olary Domain, Curnamona Province. Formerly the Weekeroo Amphibolite. No equivalent in Broken Hill Domain. Appears as Montstephens Metabasalt on p29. May be coeval with the 1719-1713 Ma Basso Suite, so previous suggestions that this unit is equivalent to the Parnell Formation, or is a unit in the Lady Louise Suite, are incorrect. Mn-enrichment in association with Bewooloo Formation.||Ethiudna Subgroup.||Interbedded with psammitic metasediment of the Bewooloo Formation.|Pillow, amygdaloidal and agglomeratic metabasalt; several metamorphosed mafic bodies.|
75186|Montstephen Metabasalt Member|64741|5|Briefly described|p304, p305|||Of the Ethiudna Subgroup? (unclear - needs checking with Conor). Large lenticular body of amygdaloidal basalt with spectacular lateral facies variations - polymict and monomict conglomerates of disaggregated pillows in a ferro-magnesian carbonate matrix||Bewooloo Formation||||02-AUG-12
75186|Montstephen Metabasalt Member|66302|6|Mentioned|p36 Fig.9, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Beewooloo Member||||
75186|Montstephen Metabasalt Member|70658|5|Briefly described|p1-3, 11-12, 27-29, 32|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province. More commonly presented simply as Montstephen Metabasalt.|1718 Ma.|Toraminga Formation.|||Amygdaloidal metabasalt, externsive volcaniclastic conglomerate, metachert.|
75186|Montstephen Metabasalt Member|73243|6|Mentioned|p59|Statherian|Statherian|Olary Domain.|ca 1710 Ma||||Includes albitised pillow lava.|
70623|Montstephen Metabasalts|62373|5|Briefly described|p502, p503|Statherian|Statherian|Subvolcanic mafic magmatic event. Pillow lavas and amygdaloidal basalts. Intercalated with the Ethiudna Subgroup rocks. Age: 1715-1700Ma.||||||
70623|Montstephen Metabasalts|64316|5|Briefly described|p534|Paleoproterozoic|Paleoproterozoic|Age: 1710-1699Ma. Geological Province: Olary Domain/Curnamona Province.||||||07-FEB-11
68061|Moody Granite Suite|24526|6|Mentioned|p99|Paleoproterozoic|Paleoproterozoic|Weakly deformed.  Age: c.1700Ma.  Part of the Kimban Orogeny.||||||07-NOV-08
34284|Moody Granitoid Suite|22690|6|Mentioned|P305|Statherian|Statherian|Age of unit is 1740 to 1700 Ma||||||
34284|Moody Granitoid Suite|22834|6|Mentioned|P39|||Same unit as the Moody Suite||||||
34284|Moody Granitoid Suite|23791|5|Briefly described|p6|Proterozoic|Proterozoic|See also Moody Suite.||||||
34284|Moody Granitoid Suite|61307|6|Mentioned|p40|Paleoproterozoic|Paleoproterozoic|Age: ~1700Ma. See also Moody Suite.||||||07-NOV-08
68957|Moody Suite granites|61070|6|Mentioned|Map Legend|||||||||12-JAN-10
41692|Moody Tank Granite|50605|5|Briefly described|p(i), 1.3, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1709 +/- 14Ma (Rb-Sr). Of the Younger Lincoln Supersuite.||||||07-NOV-08
34574|Moody Tank adamellite|22834|6|Mentioned|P39|||Reduced to Moody Tank phase of Moreenia Adamellite.||||||
28093|Moody Tank granite|24197|5|Briefly described|p74 Tb. 8.1|Paleoproterozoic|Paleoproterozoic|Informal name. Age: 1750-1700Ma.||||||07-FEB-11
34575|Moody West adamellite|22834|6|Mentioned|P39|||||||||
22369|Moolalla Member|69982|5|Briefly described|p31, p39|||Of Zang (1993), for the glauconitic sandstone lithofacies of the Pando Formation. On p39, reasons are given for abandoning this name.||||||
81754|Moolawantana Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Mis-spelling of Moolawatana Suite. Mount Painter area.|1563-1555 Ma.|||||
80363|Mooleugore Schist|63102|6|Mentioned|p15, p18|||Geological province: Olary Domain, Curnamona Province.  Superseded; see Walparuta Formation.||||||22-OCT-19
80363|Mooleugore Schist|70657|6|Mentioned|p18, p23|||Conor (2000). Subsequently the Mooleugore Formation.||||||
80364|Mooleulooloo Psammopelite|63102|5|Briefly described|p13|||Geological province: Olary Domain, Curnamona Province. See Mooleulooloo Formation.||Unit of Mount Howden Subgroup.||||
80364|Mooleulooloo Psammopelite|70657|6|Mentioned|p43|||Conor (2000); subsequently the Mooleulooloo Formation.||||||
68092|Mooleulooloo psammopelite|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Informal - see Mooleulooloo Formation. Of the Strathearn Group.  Age: <1651+/-7Ma.  Geological Province: Olary Domain.||||||28-APR-05
81706|Moolooloo Member|71129|5|Briefly described|p129|Ediacaran|Ediacaran|Of Adelaide Geosyncline.||Unit of Brachina Formation.||Correlable to Tregolana Shale Member/Tent Hill Fm.||
83638|Moomba-Big Lake Granodiorite|73479|6|Mentioned|p162|Carboniferous|Carboniferous|Uranium-rich. See also Big Lake Granodiorite p157.||||||
28770|Moonak Formation|42269|6|Mentioned|Fig.1 p335|||||||||23-AUG-18
72815|Moonan formation|23981|6|Mentioned|p23|||Informal- see Moonan Formation.||||||
38632|Moonaree Dacite|24346|6|Mentioned|p105, p104 Fig. 4|||Informal - Abbreviation of Moonaree Dacite Member.||||||
38632|Moonaree Dacite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Massive, red, commonly columnar jointed dacite, porphyritic with phenocrysts of plagioclase, pyroxene; massive, red-brown, up to 1% quartz phenocrystic dacite; massive, black, grey or brown dacite, sometimes flow-banded, welded/chilled base of flow.|
38632|Moonaree Dacite|72065|6|Mentioned|p105-106, 108-110,112,115-116|||Geological province: Gawler Craton. Informal/Misspelt use: See Moonaree Dacite Member.||Unit of Yardea Dacite.||||10-JAN-20
81707|Moonlight Conglomerate''|71129|5|Briefly described|p98,101,107|Tonian|Tonian|Of Stuart Shelf. Nomenclature of Australian Selection Pty Ltd (1979); informally used by exploration geologists to describe a thin conglomeratic to minor sandy unit between Beda Basalt and Tapley Hill Formation. Interpreted to be either part of Callanna Group (Australian Selection Pty Ltd, 1979; strat log page 44) or lower Umberatana Group (Australian Selection Pty Ltd, 1979; cross-section legends on maps between pages 61 and 62). Similar stratigraphic position to McLeay Beds and Elizabeth Creek Conglomerate.||||Underlain by Beda Basalt or Pandurra Formation or Tapley Hill Formation. Partial equivalent to Backy Point Formation.||22-NOV-19
80628|Moonta Formation|71799|4|Described|p150 fig 2|Statherian|Statherian|Eastern Gawler Craton. [misspelling? Of Moonta Porphyry].|ca 1775 Ma|Wallaroo Group||Overlain by the Matta Formation.|Silicic volcanics, porphyry.|03-OCT-18
34324|Moonta Subdomain volcanics|22629|5|Briefly described|p153|Statherian|Statherian|1765-1735 Ma.||||||07-MAR-16
69735|Moonta Volcanics|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
69735|Moonta Volcanics|60515|6|Mentioned|p116 Fig.1 |||||||||
69735|Moonta Volcanics|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
69735|Moonta Volcanics|65376|6|Mentioned|p8 Fig.1.1. |||||||||
69735|Moonta Volcanics|65390|5|Briefly described|p18, p23 Fig.3|Statherian|Statherian|Olympic Domain, Gawler Craton. Text also refers to Moonta Porphyry, probably the same unit. U-Pb age of 1760 +/- 7 Ma (U-Pb zircon; Fanning, pers. comm., 2002) given. Interbedded with Wallaroo Group.||||||
69735|Moonta Volcanics|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
69735|Moonta Volcanics|66302|6|Mentioned|p4 Fig.3, |||||||||
69735|Moonta Volcanics|69649|6|Mentioned|p6 Fig.4|||||||||23-FEB-15
41693|Moonta adamellite|24197|6|Mentioned|p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name - probably refers to same unit as Moonta monzogranite? Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
41693|Moonta adamellite|50605|5|Briefly described|p(ii), 1.3, 8.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite.||||||
37184|Moonta adamellite""|23719|6|Mentioned|p24|||||||||
33871|Moonta monzogranite|22430|6|Mentioned|p2||Proterozoic|||||||
33871|Moonta monzogranite|24197|6|Mentioned|p30|||Informal name - probably refers to same unit as Moonta adamellite? Of the Hiltaba Suite (Roxby Downs type). Geological Province: Gawler Craton.||||||07-FEB-11
26750|Moonta porphyry|33474|6|Mentioned|Fig.1|||||||||
26750|Moonta porphyry|35270|6|Mentioned|Fig.3|||||||||
26750|Moonta porphyry|39349|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26750|Moonta porphyry|73165|6|Mentioned|p620, Fig. 1|||Depicted as part of the Wallaroo Group in Fig. 1, p620.||Wallaroo Group||||
67954|Mooracoochie Volcanics, upper|44133|5|Briefly described|p31|Cambrian|Cambrian|||||||
77509|Mooracoochie volcanics|62537|6|Mentioned|p191 Fig.2. |Early Cambrian|Early Cambrian|Warburton Basin.||||||
31429|Moorilah Siltstone Member|22921|5|Briefly described|38|||Parent Sandison Subgroup||||||
31429|Moorilah Siltstone Member|43622|6|Mentioned|p38|||Misspelling of Moorillah Siltstone Member, Brachina Formation.||||||
31429|Moorilah Siltstone Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Marinoan.||Of Brachina Formation.||||
27494|Moorilyanna Conglomerate|23818|5|Briefly described|p40 Fig.11|Adelaidean|Adelaidean|Geological Province: Musgrave Block.||||||
27494|Moorilyanna Conglomerate|31970|6|Mentioned|p16|||See also P20||||||
27494|Moorilyanna Conglomerate|33478|6|Mentioned|p454|||||||||
27494|Moorilyanna Conglomerate|34537|6|Mentioned|Fig.11|||Adelaidean||||||
27494|Moorilyanna Conglomerate|35308|6|Mentioned|p454|||||||||
27494|Moorilyanna Conglomerate|39352|6|Mentioned|Map legend|Early Cambrian|Adelaidean|Early Cambrian to Marinoan||||||
27494|Moorilyanna Conglomerate|40910|6|Mentioned|p13|||||||||
27494|Moorilyanna Conglomerate|44133|5|Briefly described|p39|||Superseeded by Moorilyanna Formation.||||||
27494|Moorilyanna Conglomerate|44535|4|Described|map legend|||(G/53-9). Unit of Sturtian Series.||||||
27494|Moorilyanna Conglomerate|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Conglomerate, arkose, shale, siltstone.||||||
27494|Moorilyanna Conglomerate|61108|5|Briefly described|map legend|Cambrian|Cambrian|Conglomerate, arkose, shale and siltstone.||||||
27494|Moorilyanna Conglomerate|65376|5|Briefly described|p9 Fig.1.2. |Paleozoic|Paleozoic||||||Conglomerate, arkose, shale, siltstone.|
27494|Moorilyanna Conglomerate|68131|5|Briefly described|p2 Fig.1|Cambrian|Cambrian|Mapped with Levenger Formation as a single unit.|||||Conglomerate, arkose, shale and siltstone.|
28773|Moorland Lignite|37065|6|Mentioned|p42|||Misspelling of Moorlands?||||||
42528|Moorlands Coal Measures""|23818|6|Mentioned|p179|Late Eocene|Late Eocene|Informal name - refers to the Moorlands Lignite Member.||||||
68823|Moorna Sands|50078|6|Mentioned|p39|||||||||
81831|Moornada Sand|68131|6|Mentioned|p84|Holocene|Holocene|[Mis-spelling of Moornaba Sand].||||||
72816|Moorowie Formation, lower|23981|6|Mentioned|p58|||Informal - see Moorowie Formation.||||||
22385|Moreenia Adamellite|22834|2|Defined|p39, p40||Statherian|New formation name, includes Moody Tank adamellite and Moody West adamellite of Coin (1976), Mortimer (1984) & (Parker (1993). Age of unit is 1709+/-14 and 1692+/-10 Ma||||||28-FEB-19
22385|Moreenia Adamellite|61070|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Moody Suite. Coarse-grained grey biotite adamellite, with feldspar laths up to 100mm long. Minor Garnet. Age: 1692 +/-10Ma (U-Pb Zircon). Geological Province: Gawler Craton.||||||12-JAN-10
22385|Moreenia Adamellite|65376|5|Briefly described|p83, pp86-87. |Statherian|Statherian|Whole rock Rb¿Sr dating of the Moreenia Adamellite, Uranno Microgranite and Chinmina Monzonite gave a combined age of 1709 ±14 Ma (Mortimer, 1984).|1720 +/- 9 Ma U/Pb SHRIMP magmatic age.|Unit in Moody Suite.|||Two phases: light pink to grey, relatively homogeneous adamellite with K-feldspar, quartz, plagioclase, biotite and minor muscovite; and a more porphyritic, unfoliated adamellite with plagioclase, K-feldspar, quartz, biotite and occasional muscovite.|28-FEB-19
22385|Moreenia Adamellite|66302|6|Mentioned|p27|Statherian|Statherian||1720 +/- 9 Ma (Fanning et al, 2007)|Moody Suite||||
22385|Moreenia Adamellite|71318|5|Briefly described|p3,44|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017970 (granite) yielded an interpreted (weighted mean 207Pb/206Pb) magmatic crystallisation age of 1716+\-13 Ma. Zircon characteristics, petrography, U-Pb isotopic results and geochronological interpretation are provided.|||||Relatively homogenous, light pink to grey, coarse-grained, granoblastic textured granite that is weakly sericitised.|10-DEC-19
31516|Morgan Group|23179|5|Briefly described|p32, Fig.2||Miocene|Of the Murray Supergroup.||||||08-FEB-07
31516|Morgan Group|23226|2|Defined|p897|||Was Morgan Limestone, now raised to group status with 3 formations to clear up confusion, informal names and clarify status of Cadell Marl Lens. Of Murray Supergroup.||||||08-FEB-07
31516|Morgan Group|24563|5|Briefly described|p485|||Defined by Lukasik and James (1998) to supersede Morgan Limestone.  Current author proposes Morgan Limestone be reinstated and Morgan Group abandoned.  Geological Province: Murray Basin.||||||
31516|Morgan Group|63066|5|Briefly described|p485|||Defined within the revised stratigraphy for the Murray Supergroup (Lukasik and James 1999) - superseding Morgan Limestone of the Murray Group, nomenclature which has not been accepted. This upgrade necessitated the elevation of Murray Group to supergroup.||||||08-FEB-07
31516|Morgan Group|63460|4|Described|p839 Fig. 2b, p847|Middle Miocene|Early Miocene|Includes Finniss, Glensforlan, Cadell, Bryant Creek and Pata Formations. Geological province: Murray Basin.||||||
31516|Morgan Group|64237|5|Briefly described|p18, p19|Middle Miocene|Early Miocene|Superseded Morgan Limestone when Lukasik and James (1998) revised the Murray Group stratigraphy up to Murray Supergroup status. Subsequently demoted to Morgan Subgroup as a result of the non-acceptance of the supergroup classification.||||||
31516|Morgan Group|72445|6|Mentioned|App.6 p2 Fig.1.|Middle Miocene|Middle Miocene|Of Lukasik and James (1998) modified after Ludbrook (1961).||||Overlies Glensforian Formation and Finniss Formation.||
39835|Morgan Group""|24563|6|Mentioned|p485|||Informal - see Morgan Group.||||||
39835|Morgan Group""|63066|6|Mentioned|p485|||Informal - see Morgan Group.||||||
82043|Morgan Limestone Member|72445|6|Mentioned|App.7 p7.|Miocene|Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991) as Morgan Limestone.||Of Murray Group|||Includes thick limestone.|
72713|Morgan Limestone, Lower|62899|6|Mentioned|p50, p55|Early Miocene|Early Miocene|Informal - see Morgan Limestone.||||||
41715|Morgan limestone|50154|5|Briefly described|p135|||Of the Murray Group. Informal name.||||||
29442|Morgan-Mannum Limestone""|42966|6|Mentioned|Table 19, p131|||Informal use as synonym for Morgan Limestone||||||
28776|Morgan-Mannum limestone""|30754|6|Mentioned|p13|||Informally used where Morgan and Mannum Limestones indistinguishable||||||
80389|Morgan-Mannum limestones|71248|14|Not recorded|p2|Miocene|Miocene|||||||
35892|Morialpa Migmatite""|23347|6|Mentioned|p55|||Of Laing (1996a). Represents 'high strain zones'.||||||24-MAR-09
70595|Mornay Profile""|61825|5|Briefly described|p138|Late Cretaceous|Late Cretaceous|Informal name.  Of Idnurm and Senior (1978). Remnant weathering profile - found at margins of Eromanga Basin.||||||
69644|Morney Profile|61155|6|Mentioned|p17||Early Paleocene|See also "Morney Profile".  Geological Province: Lake Eyre Basin and southwest Queensland.||||||
69644|Morney Profile|65338|6|Mentioned|p67.|Eocene|Late Cretaceous|Weathering episode.||||||
69644|Morney Profile|66131|6|Mentioned|p242 Fig.4, p248-250, p257|||Oldest weathering phase in Lake Eyre Basin. Possibly Cretaceous to Eocene.||||Is overlain by Eyre Formation.||
69644|Morney Profile|68593|5|Briefly described|p31|Eocene|Maastrichtian|Idnurm and Senior (1978). Produced by deep weathering. Age supported by palaeomagnetic dating by McQueen et al. (2002).|60 +/- 10 Ma.|||||
41564|Morney surface|60267|6|Mentioned|p27|||Informal name.  State not certain - stated to be "in inland Australia" - probably South Australia?||||||
32310|Morum Member|70078|6|Mentioned|Northern: Fig.2. Regional: Fig.4|Late Cretaceous|Late Cretaceous||||Belfast Mudstone.|||
33228|Mount Alice Conglomerate Member|44658|14|Not recorded|map legend|||M.Tertiary. (G53-15).||||||
68905|Mount Aroona sandstone|24138|5|Briefly described|p64|||Informal. Geological Province: Adelaide Geosyncline||||||
37121|Mount Arrowsmith volcanics|23562|5|Briefly described|p292|Neoproterozoic|Neoproterozoic|Age: 586+/-7 Ma. Mount is Mt. in text. Informal?||||||
28785|Mount Barker Quartzites|30377|6|Mentioned|p201|||||||||
67955|Mount Burr group|44133|6|Mentioned|p264|||Informal name. ||||||
81616|Mount Burr volcanics|70029|5|Briefly described|p151|||Volcanism resulting in localised regional uplift and crustal doming, resulting in the higher topographical relief of the Gambier Limestone.|> c. 0.78 Ma|||||
78498|Mount Caernarvon Greywacke|67979|6|Mentioned|p530 Fig.1, p537-8|||Name used interchangeably with Mount Caernarvon Greywacke Member in this article and appears to be a casual shortening.  Of Dalgarno and Johnson (1965). ||||||
78498|Mount Caernarvon Greywacke|71237|14|Not recorded|p10|||||||||
28789|Mount Chandler Quartzite|33578|4|Described|p77|||Geology.||||||
35702|Mount Chandler Sandstone""|23282|6|Mentioned|p80|||of Coats (1963).||||||
67956|Mount Crispe beds""|44133|5|Briefly described|p4 Fig. 7.2, 42|Middle Cambrian|Middle Cambrian|Geological Province: Western Warburton Basin. Thickness: 540m.||||||
67956|Mount Crispe beds""|71342|6|Mentioned|Ch9 p4, Ch9 p9, Ch9 p11|Cambrian|Cambrian|Thermal history briefly described (Ch9 p4).||||||
69757|Mount Davies gabbro/pyroxenite intrusion|44109|4|Described|p10, p48|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Gabbroic zone intrudes felsic granulite; hybrid transition zone;  pyroxenite and olivine gabbro; serpentinised peridotite. Age: 1078+/- 3Ma (granophyre) Max. thickness: >7000m. ||||||
69757|Mount Davies gabbro/pyroxenite intrusion|61339|5|Briefly described|Map legend|||Informal name. Gabbro, gabbronorite, pyroxenite and peridotite. Thickness: >7000m.||||||21-SEP-05
76215|Mount Eba Formation|67058|6|Mentioned|p479.|||Written as Mt Eba Formation in the article. The Mt is not part of the formal name.||||||
35831|Mount Gambier Limestone""|23322|6|Mentioned|957|||Of Tennyson-Woods (1865).  Superseded - see Gambier Limestone.||||||07-SEP-09
35831|Mount Gambier Limestone""|63124|6|Mentioned|p91|||Of Tenison-Woods (1865). Changed to Gambier Limestone to reflect current usage (Sprigg 1992). ||||||
39217|Mount Gambier Stone|23731|6|Mentioned|p27|Tertiary|Tertiary|Commercial name for fossiliferous limestone of Mount Gambier area.||||||
78583|Mount Gambier Volcanic Group|68990|6|Mentioned|p459|||(Sprigg 1952; Sheard 1990, 1995) are cited. [Not recorded in the ASUD; followed this up in Sprigg (1952), who appears to have made no mention of this name; similarly Sheard (1990) refers to Mount Gambier Volcanic Complex, not Group.]||||||09-JAN-15
76008|Mount Gambier Volcanics|50133|6|Mentioned|p3 Fig.1|||||||||
69135|Mount Gambier volcanic complex|61135|6|Mentioned|p7|||Informal name.  Mount is Mt in text.||||||
83873|Mount Gee Unit|67430|6|Mentioned|p39-41, 56|||Mount Gee - Mount Painter area, Mount Painter Inlier. An informal name. See references (p39-41, 43, 56-57) to Mount Gee Sinter, the current formal version.|||||Quartz +/- hematite-rich rocks.|
40458|Mount Gee hematite breccia|24593|6|Mentioned|p625 Fig. 9|Late Ordovician|Late Ordovician|Informal name.  Mount is Mt. in text.||||||
40459|Mount Gee quartz-hematite|24593|6|Mentioned|p621|||Not intended as a formal name.  Mount is Mt. in text.||||||
29848|Mount Howden Formation|22884|2|Defined|p40 Fig. 1, p46||Paleoproterozoic|Top unit in Paragon Group (Willyama Supergroup). Underlain by Mustering Paddock Formation. Max. thickness:2000m. Pelitic, psammopelitic and lesser psammitic metasediments, fine-grained, and siliciclastic.; graphite at base and variably thro'out, + alumino||||||26-MAR-09
35887|Mount Howden Formation""|23347|6|Mentioned|p54|||Of Laing (1996a). Superseded by Mount Howden Subgroup.||||||24-MAR-09
68093|Mount Howden Subgroup, lower|60485|6|Mentioned|p29|||Informal - see Mount Howden Subgroup. Mount may be Mt in text.||||||03-MAR-05
39673|Mount Howie Sandstone Equivalents|24175|6|Mentioned|p31|Cretaceous|Cretaceous|Informal name.||||||
79314|Mount Howie Sandstone Member|69457|6|Mentioned|p41:3|Late Cretaceous|Late Cretaceous|SW Eromanga Basin. Is shown at the top of (and presumably a Member of) the Winton Formation, below an unconformity. [There is no other reference to this "Member" in the entire publication].||||||12-JUL-16
79314|Mount Howie Sandstone Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Winton Formation||
39674|Mount Howie Sandstone equivalents|24175|5|Briefly described|p17 Fig. 3|Turonian|Turonian|Informal name.||||||
25734|Mount Johns Conglomerate|22746|5|Briefly described|Fig.3 p515|Early Cambrian|Early Cambrian|Spelt Mt Johns Conglomerate||||||
25734|Mount Johns Conglomerate|23282|6|Mentioned|p77,78|||of Krieg (1973) and Benbow (1982). Redefined as a member of Apamurra Formation.||||||
25734|Mount Johns Conglomerate|23288|6|Mentioned|Fig.5||Early Cambrian|||||||
25734|Mount Johns Conglomerate|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
25734|Mount Johns Conglomerate|30544|6|Mentioned|p49|||||||||
25734|Mount Johns Conglomerate|30807|6|Mentioned|p102|||Suggested map symbol||||||
25734|Mount Johns Conglomerate|31698|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|?Middle to Upper CambrianM? - U||||||
25734|Mount Johns Conglomerate|33738|6|Mentioned|p45|||||||||
25734|Mount Johns Conglomerate|35628|4|Described|Table 3|||||||||
25734|Mount Johns Conglomerate|36096|6|Mentioned|Fig.3|||||||||
25734|Mount Johns Conglomerate|36491|6|Mentioned|Fig.2|||||||||
25734|Mount Johns Conglomerate|36920|6|Mentioned|Table 1|||||||||
25734|Mount Johns Conglomerate|38022|6|Mentioned|Fig.17|||||||||
25734|Mount Johns Conglomerate|38329|1|Redefined|p202|Cambrian|Cambrian|||||||
25734|Mount Johns Conglomerate|39352|6|Mentioned|Map legend|Late Cambrian|Early Cambrian|Early to Late Cambrian||||||
25734|Mount Johns Conglomerate|40945|6|Mentioned|Fig.3|||||||||
25734|Mount Johns Conglomerate|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Marla Group. Spelt Mt Johns Conglomerate. Fan-delta conglomerate and sandstone.||||||25-MAY-05
25734|Mount Johns Conglomerate|43258|5|Briefly described|Map Legend||Cambrian|spelt Mt. Johns Conglomerate.||||||
25734|Mount Johns Conglomerate|43298|5|Briefly described|Map Legend||Cambrian|spelt Mt Johns Conglomerate.||||||
25734|Mount Johns Conglomerate|43657|6|Mentioned|Fig.3,p4||Cambrian|||||||
25734|Mount Johns Conglomerate|43690|6|Mentioned|Fig.2,p157||Cambrian|||||||
25734|Mount Johns Conglomerate|43732|6|Mentioned|Fig.4,p5||Early Cambrian|||||||
25734|Mount Johns Conglomerate|43743|6|Mentioned|Fig.2,p33||Middle Cambrian|||||||
25734|Mount Johns Conglomerate|44109|5|Briefly described|p22 Fig. 19|Cambrian|Cambrian|Of the Marla Group. Includes the Apamurra Member. Geological Province: central Officer Basin. Mount is Mt in text of figure. ||||||
25734|Mount Johns Conglomerate|44133|4|Described|p38, 40, 4 Fig. 7.2|Middle Paleozoic|Early Paleozoic|Geological Province: Eastern Officer Basin. Maximum Thickness: 78m. Overlies Arcoeillinna Sandstone, Wallatinna Formation. Underlies: Byilkaoora Formation.||||||07-NOV-08
25734|Mount Johns Conglomerate|49792|5|Briefly described|Fig.5|||||||||
81708|Mount Laura Formation|71129|6|Mentioned|p35,37|||Geological Province: Gawler Craton. Nomenclature of SAMEDAN Oil Corporation of Australia (1985). Informal; see Wandearah Formation.||||||
39216|Mount Lofty Sandstone|23731|6|Mentioned|p27|||||||||
39216|Mount Lofty Sandstone|61237|6|Mentioned|p36|||Used as building stone, superseding the Tapley Hill and Glen Osmond Bluestones.||||||
39216|Mount Lofty Sandstone|64769|6|Mentioned|p28|||SA. Dimension stone name.||||||06-MAY-09
69737|Mount Margaret Surface|24506|5|Briefly described|p18 Fig. 4|Mesozoic|Late Paleozoic|Remnant of land surface developed upon the Mount Margaret Quartzite - until Early Mesozoic.||||||07-NOV-08
69737|Mount Margaret Surface|61836|5|Briefly described|p211|Archean|Archean|Yielded by the Bopeechee Regolith weathering event.  On the WARRINA sheet.||||||07-NOV-08
69737|Mount Margaret Surface|69023|5|Briefly described|p86|Mesozoic|Paleozoic|A remnant erosional peneplain surface in the Davenport Range. Regarded as same age as Bopeechee Regolith.||||||
69737|Mount Margaret Surface|70938|5|Briefly described|p807-808, p813-814 Figs.5 & 6, p815|Permian|Permian|Davenport Range. An erosional peneplain; late Permian. Abbreviated to MMS. Indicates exhumation from c.340 to 250 Ma.||||||
67957|Mount McDonnell Formation, upper|44133|5|Briefly described|p6|Cambrian|Cambrian|Informal name. ||||||
37143|Mount McRae Shale Formation|23612|5|Briefly described|p840|Proterozoic|Archean|Age: ~2600-2480 Ma.||||||07-NOV-08
37143|Mount McRae Shale Formation|24231|5|Briefly described|p186|||Of Hamersley Group. Geological Province: Hamersley Basin.||||||17-MAR-05
37143|Mount McRae Shale Formation|73574|6|Mentioned|p769|||Hamersley Province.||||||
35825|Mount Monster granite|23317|6|Mentioned|378|||||||||
35825|Mount Monster granite|50133|6|Mentioned|p11 Tb.2|||Informal. Sr ratios shown for Mt Monster under 'Keith area granites' heading.||||||
83692|Mount Monster rhyolite|73430|6|Mentioned|p518|Early Ordovician|Early Ordovician|Written as Mt Monster rhyolite. Misspelling of Mount Monster porphyry? [Also referred to as Mt Monster rhyolite porphyry p495.]|472.5+/-1 Ma|Padthaway Ridge suite||Unconformably overlies Kanmantoo Group||
37479|Mount Neil Granite|24045|5|Briefly described|p554 Table 1|Mesoproterozoic|Mesoproterozoic|Mount is Mt in text. Misspelt - see Mount Neill Granite||||||
37479|Mount Neil Granite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1569 Ma. Mount is Mt in text.||||||04-FEB-16
37479|Mount Neil Granite|72454|6|Mentioned|p2 Fig.2, p34, 47|Mesoproterozoic|Mesoproterozoic|Part of the Mount Painter Inlier.|||||Felsic  intrusives.|
37479|Mount Neil Granite|72461|6|Mentioned|p6||||1569 +/- 14 Ma|||||
72993|Mount Neil Granite Porphyry|63141|6|Mentioned|p542 Fig. 1|||||||||
37480|Mount Neil Granite porphyry|24045|5|Briefly described|p554 Table 1|Mesoproterozoic|Paleoproterozoic|Informal Name.||||||07-NOV-08
28121|Mount Neill Granite Porphyry|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
28121|Mount Neill Granite Porphyry|23411|6|Mentioned|Map Legend|||||||||
28121|Mount Neill Granite Porphyry|23775|5|Briefly described|p721|||Now referred to as Mount Neill Granite. Spelt 'Mt' in text.||||||22-SEP-09
28121|Mount Neill Granite Porphyry|24176|4|Described|p9, p26 Tb. 1|Proterozoic|Proterozoic|Of "Older Granite Suite". Granite porphyry, minor adamellite prophyry, granodiorite and microgranite. Age is Carpentarian. Geological Province: Mount Painter Province.||||||11-NOV-13
28121|Mount Neill Granite Porphyry|30176|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
28121|Mount Neill Granite Porphyry|30177|2|Defined|p125|Carpentarian|Carpentarian|Prob. Carpentarian. Type localities: A quarter of a mile north-northwest of Mount Neill, lat.
30degrees01'46"S long. 139degrees37'10"E. Subsidiary type locality: creek section 1.3 miles south-southwest of Mount Adams.||||||25-NOV-22
28121|Mount Neill Granite Porphyry|30807|6|Mentioned|p103|||Suggested map symbol||||||
28121|Mount Neill Granite Porphyry|30920|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
28121|Mount Neill Granite Porphyry|35255|6|Mentioned|Fig.24|||||||||
28121|Mount Neill Granite Porphyry|41403|6|Mentioned|p46|||||||||
28121|Mount Neill Granite Porphyry|42105|6|Mentioned|p88|||||||||
28121|Mount Neill Granite Porphyry|42624|5|Briefly described|p30|||||||||
28121|Mount Neill Granite Porphyry|65925|6|Mentioned|p129.|||Superseded by Mount Neill Granite.||||||
28121|Mount Neill Granite Porphyry|68068|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Subsequently the Mount Neill Granite.||||||
28121|Mount Neill Granite Porphyry|69019|6|Mentioned|p20, p27-29 Figs.7-9.|||Coats et al. (1969) included in this unit rocks which are now the Petermorra Volcanics.||||||
28121|Mount Neill Granite Porphyry|69023|5|Briefly described|p23, p46, p50|||Of Coats and Blissett (1971). Redefined as Mount Neill Granite by Teale (1993), excluding various granitoids in Mount Babbage and Mount Painter Inliers, as well as the Petermorra Volcanics.||||||
28121|Mount Neill Granite Porphyry|69650|6|Mentioned|p62, p74-75|||Coats and Blissettt (1971); revised to Mount Neill Granite by Teale (1993).||||||
28121|Mount Neill Granite Porphyry|71531|14|Not recorded|p8, 9, 10||Carpentarian|||||||
81274|Mount Neill Suite|68205|5|Briefly described|p84-86,88-90,92,94-96,99-101|||Geological province: Curnamona Province. Also described as Mount Neill Granite on p94. Dominates the Mt Painter Inlier. Geochemical analysis provided from p88-92. Nd isotope analysis on p92-94. U-Pb zircon geochronology on p94-99.  Concordant age: 1554+/-8 Ma from sample ARK20 by LA-ICPMS.|~1575 Ma||||Granites and trondjhemites, equigranular to porphyritic, and contain quartz crystals with a noticeable bluish colour; gneiss and schists and quartz-augen gneisses; rare mafic enclaves.|07-AUG-19
81274|Mount Neill Suite|72459|4|Described|p58-62, p69-70, p73, p78-81, p94-99|Mesoproterozoic|Mesoproterozoic|Mt Painter/Babbge inliers. Undeformed relative to the Box Bore granite. Petrographic descriptions of Mt Neill Suite phases are provided on p59. U-Pb dates for various constituents include 1576 +/- 2 Ma (Rhyolite from Harts Creek), 1575 +/- 14 Ma (Dacitic Tuff, Gunsight Prospect); both are derived from Teale, 1993b, Table 5.14. Rocks show generally small variations in Th(60-90ppm) and U(10-40ppm) variation in immobile elements like Zr, Nb, REE and Y is present. Rocks are interpreted to be emplaced as volcanic to subvolcanic sequences. Alteration is interpreted to have occurred some stage between 1575 Ma and 1560 Ma.|ca. 1575 Ma||Includes the Mount Neill granite, Nooldoonooldoona Trondhjemite, Pepagoona Porphyry.||Variable appearance, includes: coarse megacrystic granite/augen gneiss, medium to coarse grained granite, grey porphyritic rhyolite and grey to white or pink medium to coarse granitoids.|
37477|Mount Neill Type Granite|24045|5|Briefly described|p533 Fig.2|Proterozoic|Proterozoic|Mount is Mt in text. Informal name.||||||
40460|Mount Neill granite|24593|6|Mentioned|p619|||Informal name.  Mount is Mt. in text.||||||
40460|Mount Neill granite|72459|6|Mentioned|p59, p69|Mesoproterozoic|Mesoproterozoic||1569 +/- 14 Ma (U-Pb zircon; Teale, 1993b)|Mt Neill Suite||||
29890|Mount Painter Complex""|22857|6|Mentioned|Tb. 13.1 (insert p70-71)|Mesoproterozoic|Paleoproterozoic|Informal - see Mount Painter Complex.||||||
29890|Mount Painter Complex""|43052|6|Mentioned|p93|||||||||
73188|Mount Painter Gneiss""|63224|6|Mentioned|p12|||Interpretation has been revised: considered to be equivalent of Radium Creek Metamorphics, therefore has been labelled thus. Geological Province: Curnamona Province.||||||07-FEB-08
69044|Mount Sarah Formation|61108|5|Briefly described|map legend|Pleistocene|Paleocene|Spelt Mt on map legend. Undifferentiated early Tertiary to Plio-Pleistocene alluvial, colluvial and residual clastics, commonly silcreted or ferricreted. Geological Province: Lake Eyre Basin.||||||02-JUN-05
78857|Mount Shannon Iron Formation|66882|5|Briefly described|p103 Fig.3|Statherian|Statherian|Mount Bosanquet Region,Cleve-Port Lincoln uplands. Age from maximum depositional ages of under- and over-lying units. Correlated with Upper Middleback Jaspilite in 1993.|1790-1785 Ma.|Cleve Group||Previously considered to underlie Bosanquet Formation. Underlies Yadnarie Schist. Overlies Mangalo Schist.||16-MAY-14
72817|Mount Terrible formation|23981|6|Mentioned|p13|||Informal - see Mount Terrible Formation. Mount is Mt in text.||||||
29813|Mount Tondina Beds|43050|5|Briefly described|p26|||Actually spelt Mt Tondina Beds. Misspelling of Mount Toondina Formation||||||
79133|Mount Toondina beds|69946|6|Mentioned|p4|||Freytag (1965); raised to Formation status by Townsend and Ludbrook (1975). Presented as Mt Toondina beds in text.||||||
38115|Mount Woodroffe norite group|24301|5|Briefly described|p28|Mesoproterozoic|Mesoproterozoic|Of Camacho, 1997. Not a formal stratigraphic name.||||||
68701|Mount Woods Complex-metasediments|60954|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Banded iron formation. Geological Province: Gawler Craton.||||||07-NOV-08
34343|Mount Woods Granite|22629|6|Mentioned|fig2p147|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
83518|Mount Woods Metamorphic Complex|73155|6|Mentioned|p276|||[Structural term?] Also shown as Mount Woods Complex p266 and Mount Woods Metamorphics p285.||||||05-SEP-22
22453|Mount Woods Metamorphics|73155|4|Described|p263, p265-266, p282 Fig.13, p283-285|Paleoproterozoic|Paleoproterozoic|Gawler Craton, Mount Woods Domain, central zone. Correlated with Hutchison Group. Overprinted by NE-trending faults. Interpreted as part of polydeformed and metamorphosed basement rocks in footwall/lower plate of Mount Woods Metamorphic Core Complex. Some units have high magnetic susceptibility. See also p275, p277, p287.|ca. 1860 Ma|Mount Woods Complex|Hutchison Group equivalents|Intruded by Mirage Granite.|Migmatic paragneiss, felsic and mafic orthogneiss, paragneisses with pelitic, psammitic and calc-silicate compositions, iron formations.|
67958|Mount Wright Volcanics, upper|44133|6|Mentioned|p14|||||||||
24406|Moyles Chert Marker|40945|6|Mentioned|p3|||||||||
24406|Moyles Chert Marker|42816|6|Mentioned|p14|||Of Observatory Hill Formation.||||||13-MAR-08
75616|Moyles Creek Chert Member|65313|5|Briefly described|p578 Fig. 6|Cambrian|Cambrian|Officer Basin.||Of Observatory Hill Formation.||Underlies Oolarinna Member, overlies Parakeelya Alkali Member.||26-MAR-12
39946|Muckanippie Anorthosite|24472|5|Briefly described|p5 Tb.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Harris Greenstone Domain, Gawler Craton.||||||07-NOV-08
39946|Muckanippie Anorthosite|61659|6|Mentioned|p36 Fig.5.|||||||||
39946|Muckanippie Anorthosite|65390|6|Mentioned|p22 Fig. 3|Statherian|Statherian|Wilgena Domain, Gawler Craton. Age of about 1690 Ma inferred in Figure 3.||||||
39946|Muckanippie Anorthosite|68131|5|Briefly described|p3 Tb.1, p5, p77, 82-83|||The type area is at Lake Barry.|1871 +/- 4 Ma (max. crystallisation age).|||Is intruded by Gawler Range Volcanics.|Metamorphosed anorthosite with minor biotite and epidote, and fractures containing amphibole.|13-MAY-20
34071|Muckanippie Anorthosite Complex|22613|6|Mentioned|p14|||Formerly Muckanippie Diorite||||||
34071|Muckanippie Anorthosite Complex|61659|4|Described|pp36-40. |||Wilgena Domain, Gawler Craton. A composite intrusive complex on the western side of the Muckanippie Shear Zone, plunging steeply to the east. Correlated with Ifould Suite.||||Intruded by Hiltaba Suite.|Comprises massif (sic) anorthosite, gabbroic anorthosite, gabbro, syenite and granodiorite.|
34071|Muckanippie Anorthosite Complex|68131|6|Mentioned|p80, p82|||||||||
34341|Muckanippie Anorthosite Suite|22629|6|Mentioned|fig2p147|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28154|Muckanippie Diorite|42546|5|Briefly described|Map legend|Mesoproterozoic||Reserved S.Daly 13-DEC-83, NLR Jan 1991, but already published herein.||||||
28154|Muckanippie Diorite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
28154|Muckanippie Diorite|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: northwestern Gawler Craton.||||||07-NOV-08
28154|Muckanippie Diorite|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28154|Muckanippie Diorite|43298|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28154|Muckanippie Diorite|44695|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
28154|Muckanippie Diorite|44935|5|Briefly described|Map Legend||Proterozoic|||||||
79901|Muckannippie Anorthosite suite|66302|5|Briefly described|p23|||Age unknown but is speculated to be either part of the 1690-1660 Ma Tunkillia Suite (Teasdale, 1997; Direen et al., 2005), the ~1630 Ma St Peter Suite, or the Gawler Range Volcanics (Stewart and Foden, 2003).|||||Diorite, gabbro, anorthosite and troctolite.|07-JUL-17
37481|Mudnawatana 'Younger" Granite|24045|5|Briefly described|p554 Table 1|Ordovician|Ordovician|Informal - See Mudnawatana Granite.||||||
72790|Mudrangie Sandstone|63056|5|Briefly described|p81 Fig. 2|Middle Ordovician|Middle Ordovician|Prograding shoreline deposits. Thickness: >55m. Geological Province: Warburton Basin.||||||06-FEB-07
72790|Mudrangie Sandstone|65489|5|Briefly described|p37, p39, p96, p120|Middle Ordovician|Middle Ordovician|Eastern Warburton Basin. Over 55m thick. Potential reservoir sandstones. Appears as Mudrangle Sandstone on p96.||Unit in Innamincka Formation.||Is overlain unconformably by Big Lake Suite.||
72790|Mudrangie Sandstone|68731|6|Mentioned|p170 Fig 3.83, p170 Fig 3.83|Middle Ordovician|Early Ordovician|The rank of Member is not spelt out. > 55 m thick. Prograding shoreline depositional environment.||Of the Innamincka Formation.||||10-MAY-16
72790|Mudrangie Sandstone|69449|6|Mentioned|p34:2 Fig.34.2|Ordovician|Ordovician|Eastern Warburton Basin.||||||12-JUL-16
72790|Mudrangie Sandstone|69673|6|Mentioned|p149 fig 120|Ordovician|Ordovician|Eastern Warburton Basin.||||||
41694|Mulgathering Complex|50605|5|Briefly described|p8.6-8.7|||Geological Province: Gawler Craton & Curnamona Province. Intruded by the Hiltaba Supersuite.||||||
68063|Mulgathing complex|24526|5|Briefly described|p97 Fig. 3|Paleoproterozoic|Paleoproterozoic|Informal - see Mulgathing Complex. Age: >2400Ma.||||||07-NOV-08
73971|Mulgathing granite""|61556|5|Briefly described|p9-10 Figure|Carpentarian|Carpentarian|In Central Province - Mount Christie.||||||21-NOV-07
77854|Mullamulung Limestone|60540|5|Briefly described|p1018|Miocene|Miocene|Of Eucla Basin. Of Lowry (1970)[misspelling of Mullamullang Member]||||||
34722|Mullina komatiite|22850|5|Briefly described|p17|||Name informal||||||
68064|Mullingarra paragneiss|24526|6|Mentioned|p114|||Informal name referring to gneiss within the Mullingarra Complex.||||||
26782|Muloowurtie Clays|23818|5|Briefly described|p174 Fig.84|Late Eocene|Middle Eocene|Geological Province: St. Vincent Basin.||||||21-JAN-05
26782|Muloowurtie Clays|29833|6|Mentioned|p130|||||||||
26782|Muloowurtie Clays|33330|6|Mentioned|p151|||||||||
26782|Muloowurtie Clays|34295|6|Mentioned|p31|||Eocene||||||
26782|Muloowurtie Clays|35106|6|Mentioned|p35|||||||||
26782|Muloowurtie Clays|42731|5|Briefly described|map legend|Eocene||||||||
26782|Muloowurtie Clays|44691|4|Described|map legend|||(I/53-12). Middle Upper Eocene- Upper Eocene.||||||
26782|Muloowurtie Clays|65375|6|Mentioned|p34.|||Named by Tepper (1879); subsequently Muloowurtie Formation (Stuart 1970). ||||||
82473|Mundi Granite|72949|6|Mentioned|p35|Calymmian|Calymmian|Curnamona Province.[ Probably a misspelling of Mundi Mundi Granite, given abbreviation is MMG.]||||||
69909|Mundi Mundi Granites|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic||Age: ~1600Ma. Geological Province: Broken Hill.||||||
69909|Mundi Mundi Granites|61825|6|Mentioned|p130|Mesoproterozoic|Mesoproterozoic|Intrudes the Willyama Supergroup.||||||09-JUN-06
69909|Mundi Mundi Granites|64725|6|Mentioned|p58 Fig.2. |||||||||
69909|Mundi Mundi Granites|67540|6|Mentioned|p27|||Of Page, Conor and Jagodzinski (in prep.). Informal name for some of the granites in the NSW portion of the Curnamona Province  considered to be part of the Ninnerie Supersuite.|||||Quartz-K-feldspar-biotite-muscovite granite.|04-FEB-16
69909|Mundi Mundi Granites|67621|6|Mentioned|p224|||Curnamona Province.||||||
69909|Mundi Mundi Granites|73165|6|Mentioned|p637, Fig. 12|||Curnamona Province.||||||
81691|Mundi-Mundi granite|63102|6|Mentioned|p51|||See Mundi Mundi Granite.||||||
33815|Munjeela Granite|24505|5|Briefly described|p5 Fig. 1|||Geological Province: Gawler Craton.||||||
33815|Munjeela Granite|24583|6|Mentioned|p12|||Geological Province: Gawler Craton.||||||
33815|Munjeela Granite|60484|5|Briefly described|p33 Fig. 1|Calymmian|Calymmian|Age: ~1590Ma. Geological Province: Gawler Craton. See also p38.||||||
33815|Munjeela Granite|60515|6|Mentioned|p116 Fig.1 |||||||||
33815|Munjeela Granite|61522|5|Briefly described|p5 Fig.1|||Geological Province: Gawler Craton.||||||
33815|Munjeela Granite|61659|6|Mentioned|p30 Fig.1. |Mesoproterozoic|Mesoproterozoic|||||||
33815|Munjeela Granite|61864|5|Briefly described|p16 fig 3, p17|||Undeformed.|~1560 Ma (Ferris, 2001).|||||
33815|Munjeela Granite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: ~1565Ma. Geological Province: Gawler Craton (Nuyts Domain).||||||10-AUG-07
33815|Munjeela Granite|64130|4|Described|p1378 Fig.1, p1380 Fig.2, p1383 |Mesoproterozoic|Mesoproterozoic|SW Gawler Craton. Derived from melting of juvenile metasedimentary rocks. U-Pb monzanite age.|ca. 1585 Ma (Payne et al., 2007).|||Intrudes St. Peter Suite.|Unfractionated, restite-rich, garnet-muscovite +/- tourmaline-bearing S-type granite.|
33815|Munjeela Granite|64576|6|Mentioned|p625 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: c. 1580Ma.||||||
33815|Munjeela Granite|64722|6|Mentioned|Fig. 5 p.13|Mesoproterozoic|Mesoproterozoic|Of South Australian Craton.||||||
33815|Munjeela Granite|64739|6|Mentioned|p264 Fig.1, |Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
33815|Munjeela Granite|64740|5|Briefly described|p284 Fig.1, p285 Fig.2, p287.|Mesoproterozoic|Mesoproterozoic|S-type granites.|1562 +/- 15 Ma EPMA of monazite.|||Intrudes St Peter Suite.|Medium- to coarse-grained, grey, equigranular, muscovite-biotite-garnet granite; syenogranite; adamellite. Contains enclaves of pelitic sediments.|26-FEB-13
33815|Munjeela Granite|65220|6|Mentioned|p19 Fig.1|Proterozoic|Proterozoic|||||||10-DEC-09
33815|Munjeela Granite|65376|6|Mentioned|p8 Fig.1.1, p155 Fig.5.1. |||||||||
33815|Munjeela Granite|65390|5|Briefly described|p22 Fig. 3|Calymmian|Calymmian|Nuyts Domain, Gawler Craton. Age of 1565 Ma given.||||||
33815|Munjeela Granite|65922|6|Mentioned|p13 Fig. 4|||Gawler Craton.||||||
33815|Munjeela Granite|66302|6|Mentioned|p4 Fig.3, p34, p46|||Ages derived from Ferris (2001) and Payne et al. (2007), respectively. |1585 Ma to 1562 +/- 15 Ma|Hiltaba Suite||||
33815|Munjeela Granite|66519|5|Briefly described|p31.|Mesoproterozoic|Mesoproterozoic|Informal term for peraluminous, S-type granites exposed at Munjeela Rockhole (inf. n.), Point Bell and Point Sinclair. Coeval with Gawler Range Volcanics - Hiltaba Suite magmatic event. Now replaced by Munjeela Suite. For new definition, see Munjeela Suite.|||||Massive to foliated, two mica +/- garnet, granites.|05-SEP-19
33815|Munjeela Granite|67058|6|Mentioned|p477 Fig. 1|Mesoproterozoic|Mesoproterozoic||1580 Ma|||||
33815|Munjeela Granite|67181|5|Briefly described|p616 Fig.1|Mesoproterozoic|Mesoproterozoic|Gawler Craton. References: Fairclough et al. 2003, Payne et al. 2003.|ca 1580 Ma|||||
33815|Munjeela Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.||||||
33815|Munjeela Granite|67536|5|Briefly described|Map Legend|Calymmian|Calymmian|Gawler Craton.|ca. 1565 Ma||||S-type granite.|
33815|Munjeela Granite|69004|6|Mentioned|p18|||Gawler Craton.||||||
33815|Munjeela Granite|69649|5|Briefly described|p29-30, p6 Fig.4, p7, p9, p36, p41-42|Mesoproterozoic|Mesoproterozoic|New name. Various ages discussed. Dating was done on monazite rather than zircon.|1562 +/- 15 Ma. Berry, CODES, (2001).||||Medium- to coarse-grained, grey, equigranular, muscovite-biotite(-garnet) granite, syenogranite to monzogranite. Includes enclaves of schist. S-type.|26-FEB-15
33815|Munjeela Granite|70893|5|Briefly described|p3 fig 1b, p76, p77|Calymmian|Calymmian|Occurs as a large coastal outcrop east of Point James. Petrography discussed in detail. |c. 1575 Ma||||Pale grey to cream, medium to coarse-grained, massive and seriate textured to locally porphyritic granite.|
33815|Munjeela Granite|71859|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|||||||
33815|Munjeela Granite|72462|6|Mentioned|p3|Mesoproterozoic|Mesoproterozoic|Gawler Craton.||||||
33815|Munjeela Granite|73302|6|Mentioned|p34|Mesoproterozoic|Mesoproterozoic|||||||
78975|Munjeena Formation|69649|5|Briefly described|p32|Neogene|Paleogene|[Mis-spelling of Munjena]. Eucla Basin. Up to 3m thick. Blankets interfluves and paleochannels around the margin of the Basin.|||||Poorly sorted conglomeratic sand, clayey sand and breccia; commonly contains rounded quartz pebbles; silicified to pedogenic silcrete.|15-JAN-15
78576|Munkarie beds""|68731|6|Mentioned|p200 Fig 3.110, p207|Lopingian|Guadalupian|Cooper Basin.||Included in basal part of the Toolachee Formation.||||12-MAY-16
78576|Munkarie beds""|70823|6|Mentioned|p70|Late Permian|Permian|APP4.3 palynofloras (older than Toolachee Formation APP5 floras). In both Qld and SA. Appears to have been incroporated into the base of the Toolachee Formation, extending the base age.||||||31-JAN-18
35698|Munta Limestone|23282|6|Mentioned|p66|||of Sukanta (1993). Now superceded by Munta Limestone Member.||||||
77778|Munyallina beds|67180|6|Mentioned|p608|Cryogenian|Cryogenian|Of Mawson (1934). Coats and Blisset (1971) and Mawson (1934) - units 3,4,5,6 and 7 of the Munyallina beds correspond to the lower algal limestones and upper oolitic dolomites of the Balcanoona Formation.||||Corresponds to the Balcanoona Formation.||
24411|Murrana Beds|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
24411|Murrana Beds|23054|5|Briefly described|p11|||||||||
24411|Murrana Beds|36733|2|Defined|p70|early Adelaidean|early Adelaidean|See also p36.||||||16-DEC-20
24411|Murrana Beds|37854|6|Mentioned|Table 1|||||||||
24411|Murrana Beds|38108|6|Mentioned|Table 1|||||||||
24411|Murrana Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24411|Murrana Beds|40294|6|Mentioned|Table 2|||||||||
24411|Murrana Beds|41403|6|Mentioned|p66|||||||||
24411|Murrana Beds|41404|5|Briefly described|p88|||||||||
24411|Murrana Beds|43052|5|Briefly described|p177,Table 6.2|||Emeroo Subgroup||||||
24411|Murrana Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24411|Murrana Beds|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|Appears in Fig.9 without the lithology/rank.||Unit in Emeroo Subgroup.||||
29466|Murravian Series|23226|6|Mentioned|p889|||Of Sturt (1833) and Tate (1878,1885).||||||10-SEP-19
29466|Murravian Series|42966|5|Briefly described|p408|||Used by Tate, 1878.||||||
42317|Murray Bridge Freestone|60566|5|Briefly described|p28-29|||Commercial name for sandy limestone quarried from the Sunnyside Quarry, north of murray Bridge. Not intended as formal name.||||||18-MAR-05
42317|Murray Bridge Freestone|61525|5|Briefly described|40|||Commercial name for the superior building stone quarried from Mannum Limestone. Sees also Murray Bridge Limestone. A durable, fine-grained fossiliferous limestone displaying a variety of colours, ranging from white to buff, yellow and tan-brown.||||||02-JUN-06
40360|Murray Group Limestones|10010|6|Mentioned|p15|||Of Brown and Stephenson (1991) and Macphail et al (1993). Formal name is Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
40360|Murray Group Limestones|23921|5|Briefly described|p1109|Early Miocene|Early Miocene|Geological Province: Murray Basin.||||||
40360|Murray Group Limestones|64961|5|Briefly described|p269 Fig. 9|Middle Miocene|Middle Miocene|Informal name - see Murray Group.||||||21-APR-09
40360|Murray Group Limestones|66287|5|Briefly described|Fig 2,4, p28 Fig. 5, p31|Middle Miocene|Middle Miocene|South Australian equivalent of the Victorian Duddo Limestone.||||Underlies the Loxton-Parilla Sands.||20-APR-12
28835|Murray Group limestone|40003|6|Mentioned|p40|||||||||
28835|Murray Group limestone|50154|6|Mentioned|p134 Fig. 6.57|||Informally referring to the limestone of the Murray Group.||||||31-AUG-04
28835|Murray Group limestone|64237|6|Mentioned|p19|||Informal name for the Duddo Limestone of the Murray Group - written as "Murray Group limestone".||||||15-JUL-08
28835|Murray Group limestone|68716|6|Mentioned|p39 Fig.3, p40, p41|||Confined aquifer.||||||
69741|Murray Range Peridotite|61341|5|Briefly described|Map legend|||Presented as the compound name Murray Range Pyroxenite/Peridotite.||||||
69763|Murray Range pyroxenite/peridotite/gabbro intrusion|44109|4|Described|p10, p81-84|Mesoproterozoic|Mesoproterozoic|Informal part of the Giles Complex. Gabbroic rocks, extensively recrystallised, to mafic granulite; contains relict layers of felsic granulite and granitic gneiss. ||||||
69763|Murray Range pyroxenite/peridotite/gabbro intrusion|61339|5|Briefly described|Map legend|||Informal name. Thickness: ~2600m.||||||
39201|Murray River limestones|23768|6|Mentioned|p33|||Informal name.||||||
31515|Murray Supergroup|23179|5|Briefly described|p32, Fig.2|Middle Miocene|Late Oligocene|Murray Basin.||||||
31515|Murray Supergroup|23226|4|Described|p890|Miocene|Oligocene|New name for Murray Group including the Ettrick Formation, Winnambool Formation and Geera Clay.||||||
31515|Murray Supergroup|24558|5|Briefly described|p653|Miocene|Oligocene|Geological Province: Murray Basin.||||||
31515|Murray Supergroup|24563|5|Briefly described|p485|Middle Miocene|Late Oligocene|Elevation to supergroup status proposed by Lukasik and James (1998).  Now abandoned and reinstated as Murray Group.  Geological Province: Murray Basin.||||||
31515|Murray Supergroup|60540|5|Briefly described|p998-1002,p1008,p1009 Fig.5|Miocene|Oligocene|Lukasik and James (1998). Previously Murray Group.||||Is overlain (onlapped) by Bookpurnong Formation.|Includes karstified and variably indurated limestones.|06-FEB-18
31515|Murray Supergroup|63066|5|Briefly described|p485-486|||Revised stratigraphic nomenclature of Lukasik and James (1999) elevated Murray group to supergroup status. This gave rise to controversy between geologists and has not been accepted. Geol Prov: Murray Basin.||||||14-AUG-08
31515|Murray Supergroup|63460|5|Briefly described|p839 Fig. 2b, p847|Middle Miocene|Late Oligocene|Comprises carbonate units including Duddo Limestone (Vic) - av. thickness of >100m, which is a direct lateral equivalent of Mannum, Finniss, Glensforlan, Cadell, Pata and Bryant Creek Fms in S. A. Therefore suggested that Duddo Limestone be abandoned.||||||
31515|Murray Supergroup|64237|5|Briefly described|p17-20|Middle Miocene|Early Miocene|Upgrade of Murray Group by Lukasic and James (1998). However, the stratigraphic revision was not generally accepted and the Murray Group has been reinstated as the current nomenclature. Geological province: Murray Basin.||||||
31515|Murray Supergroup|68548|5|Briefly described|p13 Fig.2|Miocene|Miocene|||||Is overlain unconformably by Bookpurnong and Norwest Bend Formations.|Includes limestones.|
31515|Murray Supergroup|72445|6|Mentioned|App.6 p1, p2 Fig.1, p4, p6-7.|Middle Miocene|Late Oligocene|Of Gallagher and Gourlay (2007). This name only used in App.6. See Murray Group. Samples include bryozoans, molluscs and sponge spicules.|||Includes Geera Clay, Ettrick Formation, Mannum Formation, Finniss Formation, Glensforian Formation, Cadell Formation, Pata Formation, Bryant Creek Formation.|Unconformably overlies Renmark Group.|Includes limestone, marl and marly limestone, clay and calcareous clay with sand, lignite and planktic and benthic foraminifera.|
29903|Musgrave Complex""|43052|6|Mentioned|p156|||||||||
29901|Musgrave-Mann Complex""|43052|6|Mentioned|p156|||||||||
29902|Musgrave-Mann Metamorphics""|43052|6|Mentioned|p156|||||||||
75370|Musgravian Gneiss|64722|5|Briefly described|p16-17, 27|Calymmian|Calymmian|Of Edgoose et al (2004). Of the Musgrave Orogen. Not clear if this is equivalent to, or part of, the Birksgate Complex. Formed in a collision-related environment. Contains mostly 1600-1540 Ma, but rare 1500 Ma, zircons.||||||
75370|Musgravian Gneiss|64745|5|Briefly described|p372, p373 Fig. 3, p374 Tab.1|Calymmian|Calymmian|Not a formal stratigraphic unit. Age: ca. 1.60-1.54 Ga (U-Pb SHRIMP). Geol Prov: Musgrave Province. Also known as Birksgate Complex (within Fregon Domain) or Olia gneiss (within Mulga Park Domain). Felsic composition. See also Musgravian Gneisses.||||||
75370|Musgravian Gneiss|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
75370|Musgravian Gneiss|70083|6|Mentioned|p206|||The oldest recognised lithology in the eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Birksgate Complex in the Fregon Subdomain (of the Inlier), and the Olia Gneiss in the Mulga Park Subdomain. A volcano-sedimentary sequence.|1600-1540 Ma (protoliths).||||Predominantly felsic orthogneiss, subordinate interlayered mafic units, and rare metapelite, quartzite and calc-silicate.|
75371|Musgravian Gneisses|64745|5|Briefly described|p372, p380-382|||Collective term referring to multiple gneisses of similar age. Magmatic/volcanic rocks (dominant felsic, subordinate mafic); subordinate metasediments (metapelite, quartzite layers, calcsilicates). Geol. Prov: Musgrave Province. See Musgravian Gneiss.||||||18-SEP-09
42422|Musgravian Granitoids|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Informal name referring to graniotoid suites formed during the Musgravian Orogeny. Includes Kulgera, Umutja, Pottyu, Kulpittaja and Angatja Suites. Geological Province: Musgrave Block.||||||21-DEC-04
42413|Musgravian granitoids|24496|6|Mentioned|p73|||Informal - see Musgravian Granitoids.||||||
42413|Musgravian granitoids|60662|5|Briefly described|Map Legend|||||||||22-FEB-05
73546|Mussel Member""|63124|6|Mentioned|p90|||Of Blake (1980). Interpreted to be offshore bars in the Dilwyn Formation. ||||||
39880|Mutijulu Arkose|24496|5|Briefly described|p21 Tb.2|Cambrian|Cambrian|Geological Province: Amadeus Basin.||||||
39880|Mutijulu Arkose|24499|6|Mentioned|Map legend|||||||||
39880|Mutijulu Arkose|60660|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Non-magnetic molasse basin sediments. Misspelt.||||||22-FEB-05
39880|Mutijulu Arkose|60662|5|Briefly described|Map Legend|||Molasse basin sediments. Note: misspelt.||||||22-FEB-05
39880|Mutijulu Arkose|61306|5|Briefly described|p11, p30, p53|Cambrian|Cambrian|At Uluru. Geological province: Amadus Basin. See also p46 Fig.10.||||||
39577|Nairne Pyrite Beds|24465|5|Briefly described|p346 Fig.3|||Of the Brukunga Formation, then superseded by Nairne Pyrite Member (Talisker Calc-Silicate).  Both names now abandoned.||||||19-JAN-05
69046|Nairne Pyritic Schist|60712|5|Briefly described|p33|Early Cambrian|Early Cambrian|Basal band now defined as Nairne Pyrite Member. Two thick pyrite bands first mapped by Sprigg and Wilson (1954); then by Kleeman and Skinner (1959)who incorporated two main sulphide bands and several minor bands into Nairne Pyritic Formation.||||||31-MAY-05
82981|Namba carbonate|73251|5|Briefly described|p39, p48, p52|||e.g., Marsland-Smith et al. (2011). [Article refers to this name as a term reported elsewhere; inferred to mean it is not widely used].|||||Includes or may include whitish palygorskitic dolomite.|
26317|Nankabunyana Formation|38926|2|Defined|p33|Late Precambrian|Late Precambrian|||||||
26317|Nankabunyana Formation|41404|6|Mentioned|p98|||||||||
26317|Nankabunyana Formation|42236|5|Briefly described|p107|||See also Fig.2||||||
26317|Nankabunyana Formation|42238|6|Mentioned|p73|||||||||
76009|Naracoorte Member|50133|6|Mentioned|p6 Tb.1, p8 Tb.1, p11 Tb. 2|||Major & trace element geochemistry for 2 samples given||Of the  Mount Gambier Limestone||||
39194|Naracoorte limestone|23768|6|Mentioned|p155|||Informal name - See Naracoorte Limestone.  Geological Province: Gambier Basin.||||||10-MAR-05
39194|Naracoorte limestone|50154|6|Mentioned|p135|||Informal name.||||||
40403|Narllaby Formation|24606|6|Mentioned|p958 Fig. 3|||Misspelt - see Narlaby Formation. Formation is Fm in text.||||||
24424|Nathaltee Formation|38926|2|Defined|p29|Late Precambrian|Late Precambrian|||||||
24424|Nathaltee Formation|41404|6|Mentioned|p98|||||||||
24424|Nathaltee Formation|42236|5|Briefly described|p107|||||||||
24424|Nathaltee Formation|42238|6|Mentioned|p73|||||||||
34743|Nelshaby sandstone facies""|22889|4|Described|p33|Adelaidean|Adelaidean|Informal name suggested, intending to supersede the former name Nelshaby Sandstone.  The unit occupies the upper part of the Rhynie Sandstone.||||||
28859|Nepabuna Siltstone|36198|6|Mentioned|Fig.I.2|||Misspelling of Nepabunna ?||||||
28859|Nepabuna Siltstone|37326|6|Mentioned|p3|||||||||
28859|Nepabuna Siltstone|42458|5|Briefly described|Fig.2 P699|||||||||
38733|Neridup Limestone|24397|6|Mentioned|p238 Fig. 5|||Possibly referring to location of Nanarup Limestone.  Geological Province: Eucla Basin.||||||
38733|Neridup Limestone|69598|6|Mentioned|p10|||||||||
24430|Niggly Gap Beds|22926|6|Mentioned|43|||Geol province Worumba Anticline||||||
24430|Niggly Gap Beds|37854|6|Mentioned|p11|||||||||
24430|Niggly Gap Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24430|Niggly Gap Beds|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24430|Niggly Gap Beds|39490|6|Mentioned|p10|||||||||
24430|Niggly Gap Beds|40225|3|Fully described|Map sheet|||||||||
24430|Niggly Gap Beds|40294|3|Fully described|p16|||||||||
24430|Niggly Gap Beds|41403|5|Briefly described|p67|||||||||
24430|Niggly Gap Beds|41404|6|Mentioned|p73|||||||||
24430|Niggly Gap Beds|42222|6|Mentioned|Table 1 P5|||||||||
24430|Niggly Gap Beds|42882|5|Briefly described|p4|||of Callanna Group||||||
24430|Niggly Gap Beds|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
24430|Niggly Gap Beds|43742|6|Mentioned|p43|||||||||
24430|Niggly Gap Beds|43845|6|Mentioned|p43||Neoproterozoic|In Curdimurka Subgroup. Willouran age.||||||12-JUL-16
24430|Niggly Gap Beds|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup. Grey, micaceous siltstone and fine-grained sandstone, partly with halite casts, heavy-mineral-laminated sandstone, minor dolomite.||||||29-APR-05
24430|Niggly Gap Beds|72492|6|Mentioned|p2 Fig.1, p2|Neoproterozoic|Neoproterozoic|In the Worumba Anticline.||Curdimurka Subgroup||Overlies Wirrawilka Beds and underlies Arkaba Hill Beds.|Includes desiccation cracks and ripples.|
24430|Niggly Gap Beds|73222|6|Mentioned|p7|Tonian|Tonian|Flinders Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Unconformably underlain by Wirrawilka Beds. unconformably overlain by Arkaba Hill Beds. Possibly equivalent to Recovery Formation.||
24430|Niggly Gap Beds|74367|5|Briefly described|p7 Fig.6, p9, p12-14, p20|Neoproterozoic|Neoproterozoic|Detrital zircon MDA is much older than true depositional age.|1616+/-34 Ma LA-ICP-MS detrital zircon|Curdimurka Subgroup||||
27296|Nilpinna Beds|23054|5|Briefly described|p11|||||||||
27296|Nilpinna Beds|36733|2|Defined|p69|early Adelaidean|early Adelaidean|See also P33.||||||
27296|Nilpinna Beds|37854|6|Mentioned|p11|||||||||
27296|Nilpinna Beds|38108|6|Mentioned|Table 1|||||||||
27296|Nilpinna Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
27296|Nilpinna Beds|40294|6|Mentioned|Table 2|||||||||
27296|Nilpinna Beds|43052|5|Briefly described|p175,Table 6.2|||of Curdimurka Subgroup. Peake & Denison Inliers.||||||12-FEB-09
27296|Nilpinna Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
27296|Nilpinna Beds|64796|6|Mentioned|p190 Fig.8|Neoproterozoic|Neoproterozoic|Appears in Fig.8 without the lithology/rank.||Unit in Curdimurka Subgroup.||||
76769|Ninnerie Suite|63866|6|Mentioned|p37, p49|||||||||
76769|Ninnerie Suite|64722|6|Mentioned|Fig. 2 p3-6, p14|Calymmian|Calymmian|Curnamona Province? Contains S-type granites that range in age from 1595-1580 Ma.||||||11-APR-12
76769|Ninnerie Suite|67323|5|Briefly described|p36|||Southern Curnamona Province. Emplaced towards the end of the Olarian Orogeny.|~1590 Ma.|||||
76769|Ninnerie Suite|70000|5|Briefly described|p39|||Curnamona Province. Related to iron oxide-associated Cu-Au-U mineralisation.|1600-1570 Ma.|||||
39173|Ninnes Member|24475|6|Mentioned|p53|||Of Zang (2002). Now included in the Wokurna Member of Wandearah Formation. Accidently used in Fig. 2 instead of Wokurna Member.||||||05-DEC-11
39173|Ninnes Member|65375|5|Briefly described|p19.|Paleoproterozoic|Paleoproterozoic|||Unit in Wandearah Formation.|||Interlayered albitite, siltstone, sandstone, carbonate.|
39173|Ninnes Member|65376|6|Mentioned|p101 Fig.3.1.|||||||||
25345|Noarlunga Limestone|30250|6|Mentioned|Table 2|||Refers Crespin(1954)||||||
25345|Noarlunga Limestone|35689|6|Mentioned|p18|||||||||
25345|Noarlunga Limestone|40969|6|Mentioned|Fig.1|||||||||
26278|Nonning Rhyodacite|22629|6|Mentioned|p162|||||||||
26278|Nonning Rhyodacite|22873|6|Mentioned|P10|||||||||
26278|Nonning Rhyodacite|24346|6|Mentioned|p111 App 1, p98 Fig.1|||Supserseded by Eucarro Rhyolite Formation.||||||
26278|Nonning Rhyodacite|24474|5|Briefly described|p36 Fig. 1|||Of the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
26278|Nonning Rhyodacite|40430|2|Defined|p6|Mesoproterozoic|Mesoproterozoic|||||||
26278|Nonning Rhyodacite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
26278|Nonning Rhyodacite|42283|6|Mentioned|Fig.5 P82|||||||||
26278|Nonning Rhyodacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26278|Nonning Rhyodacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26278|Nonning Rhyodacite|43052|5|Briefly described|p109|||of Gawler Range Volcanics||||||
26278|Nonning Rhyodacite|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Gawler Range Volcanics. Acid volcanics.||||||26-MAY-05
26278|Nonning Rhyodacite|43258|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26278|Nonning Rhyodacite|43298|6|Mentioned|Map Legend||Mesoproterozoic|||||||
26278|Nonning Rhyodacite|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: 1592-1589Ma. Of the Lower Gawler Range Volcanics.||||||26-APR-05
26278|Nonning Rhyodacite|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Gawler Range Volcanics, Lower. Age: 1592-1589 Ma.||||||23-JUN-05
26278|Nonning Rhyodacite|65922|5|Briefly described|p16-20|Calymmian|Calymmian|Subsequently included in Eucarro Rhyolite. Basal unit of the 'younger' or 'upper' Gawler Range Volcanics in the YARDEA sheet. Massive reddish brown porphyritic dacite grading to dacite. Thickness to 300 m. Conformably overlies Bittali Rhyolite; underlies Yannabie Rhyodacite; conformably underlies Eucarro Dacite. REE patterns imply common genesis with Eucarro and Yardea Dacites.||||||22-MAY-14
26278|Nonning Rhyodacite|69649|6|Mentioned|p17|Mesoproterozoic|Mesoproterozoic|Part of mature (upper) phase of Gawler Range Volcanics.||Unit in Gawler Range Volcanics.||||26-FEB-15
26278|Nonning Rhyodacite|71129|6|Mentioned|p85,88,90|Calymmian|Calymmian|Geological Province: Gawler Craton.||||Correlable with Eucarro Rhyolite.||
26278|Nonning Rhyodacite|71317|6|Mentioned|p56|||||||||
26278|Nonning Rhyodacite|72459|5|Briefly described|p17, p47|Mesoproterozoic|Mesoproterozoic|Large volume unit interpreted to be ignimbritic in origin with minor interbedded lavas. Part of the 'mature' phase of the Gawler Range Volcanism.||Gawler Range Volcanics||||
38628|Nonning Rhyodacite""|24346|5|Briefly described|p99|||Now included in Eucarro Rhyolite.||||||
80113|Nonning Rhyolite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Massive, red to pink, columnar-jointed rhyolite; with scattered granitoid and lithic megacryst-bearing clasts.|
73832|Nooldoonooldoona pegmatite|24546|5|Briefly described|p2 - 6 Tb.1|Paleozoic|Paleozoic|Informal. Geological Province: Mount Painter Basement.||||||07-NOV-08
82475|Nooldoonooldoona trondjhemite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Mount Painter.|1576 Ma|||||
26081|North Maslin Sand Member|30250|6|Mentioned|Table 2|||See also Table 3||||||
26081|North Maslin Sand Member|35689|2|Defined|p12|middle Eocene|middle Eocene|||||||
26081|North Maslin Sand Member|36127|5|Briefly described|p9|||||||||
26081|North Maslin Sand Member|36244|6|Mentioned|p2|||Redefined by Cooper 1979.||||||
26081|North Maslin Sand Member|38621|6|Mentioned|Table 1|||Refers Cooper 1979.||||||
26081|North Maslin Sand Member|40969|6|Mentioned|Fig.1|||||||||
26081|North Maslin Sand Member|41495|4|Described|p42|||||||||
26081|North Maslin Sand Member|41513|5|Briefly described|Fig.5|||||||||
26081|North Maslin Sand Member|41517|6|Mentioned|p141|||||||||
26081|North Maslin Sand Member|42093|5|Briefly described|Fig.2 P6|||||||||
83144|Norwest Bend Formation, lower|73228|5|Briefly described|p59|Pliocene|Pliocene|Of Miranda et al (2008). Murray Basin. Considered laterally equivalent to the 'Loxton-Parilla Sands' of Brown and Stephenson (1991). [lower is used less frequently than upper, and presumably refers to strata of the formation underlying the oyster coquinas].|~4.2 - 5.3 Ma||||Sandy, oyster-rich sediments.|
83145|Norwest Bend Formation, upper|73228|5|Briefly described|p50, p59, p61|Pleistocene|Late Pliocene|Of Miranda et al (2008). Murray Basin, western. [upper is used frequently, presumably in reference to the oyster coquinas that cap the unit].||||Disconformably underlain by 'Loxton-Parilla Sands'.|Oyster coquinas.|
29467|Norwest Bend beds|42966|5|Briefly described|p408|||Superseded by Norwest Bend Formation.||||||
79409|Nuccaleena Dolostone|69438|6|Mentioned|p23:17|||Adelaide Fold Belt.||||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
75063|Nuccaleena Limestone|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
75063|Nuccaleena Limestone|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
81632|Nue Sandstone''|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Torrens Hinge Zone. Of Adelaide Geosyncline.||||Overlain by Tapley Hill Formation. Underlain by Yeltacowie Sandstone.||16-SEP-19
28879|Nullarbor Sandstone|42086|5|Briefly described|Fig.2 p4|||||||||08-OCT-15
67947|Nullaware Greensand Member|44133|6|Mentioned|p146|||||||||
80254|Nultaddy Seismic Unit|70938|5|Briefly described|p807, p814|Devonian|Devonian|Informal name [despite capitals?]. Described as "poorly studied". Detected in seismic sections in the Boorthanna Trough.|||||Shale.|
81709|Nutt Knob Kimberlite''|71129|6|Mentioned|p135|Early Jurassic|Early Jurassic|Geological Province: Gawler Craton. Kimberlite intrusion is synchronous with tholeiitic basalts which extend parallel to the Pacific-facing subduction margin of Gondwana on Kangaroo Island, Tasmania, Antarctica and Africa. Intruded directly at the periphery of the interpreted melted mantle zone which produced these tholeiitic melts (Foden et al., 2008). Discovered via heavy mineral sampling at Nutt Knob SE of the MSDP02 drillhole, which showed the area is shedding kimberlitic indicator minerals. No outcrops were located (Helix Resoruces NL, 1999).||||||
41695|Nuyts granite|24197|6|Mentioned|p74 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name probably referring to Nuyts Volcanics. Age: 1592Ma. Geological Province: Gawler Craton.||||||07-FEB-11
41695|Nuyts granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Roxby Downs suite.||||||
75481|Oakdale Granite Gneiss|63866|5|Briefly described|p38|||[Replaced by the Georges Bore Granite].||Silver City Suite||Intrudes the Thackaringa Group and/or the Broken Hill Group.||
75481|Oakdale Granite Gneiss|66302|6|Mentioned|p41|Statherian|Statherian|Shown as Oakdale Granite Gneiss (Georges Bore Granite).|1695 +/- 4 Ma |Silver City Suite||||07-JUL-17
75481|Oakdale Granite Gneiss|72461|6|Mentioned|p16 fig 9||||1695 +/- 4 Ma|||||
26089|Observatory Hill Beds|22613|4|Described|p17|Neoproterozoic|Neoproterozoic|Officer Basin||||||
26089|Observatory Hill Beds|24067|5|Briefly described|p242|Paleozoic|Paleozoic|Geological Province: Officer Basin.||||||07-NOV-08
26089|Observatory Hill Beds|30540|6|Mentioned|p68|||Marine unit in Officer Basin||||||
26089|Observatory Hill Beds|30544|6|Mentioned|p47|||||||||
26089|Observatory Hill Beds|30807|6|Mentioned|p102|||Suggested map symbol||||||
26089|Observatory Hill Beds|30874|6|Mentioned|p5|||Discovery of Biconulites. See also P6-8||||||
26089|Observatory Hill Beds|31697|6|Mentioned|p7|||M.Cambrian||||||
26089|Observatory Hill Beds|31698|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|?Middle to Upper CambrianM? - U||||||
26089|Observatory Hill Beds|31914|5|Briefly described|p97|||Some outcrops regarded as Wanna Beds.? Cambrian||||||
26089|Observatory Hill Beds|31969|6|Mentioned|p9|||Refers Wopfner (1969)||||||
26089|Observatory Hill Beds|32204|5|Briefly described|p5|||Cambrian. Refraction survey||||||
26089|Observatory Hill Beds|32205|6|Mentioned|p15|||||||||
26089|Observatory Hill Beds|33468|6|Mentioned|Fig.3|||See also P204||||||
26089|Observatory Hill Beds|33523|4|Described|p19|||||||||
26089|Observatory Hill Beds|34610|2|Defined|p171|Cambrian|Cambrian|See also PP172 - 185||||||
26089|Observatory Hill Beds|35149|5|Briefly described|Table.1|||||||||
26089|Observatory Hill Beds|35628|4|Described|Table 3|||||||||
26089|Observatory Hill Beds|35772|6|Mentioned|p8|||||||||
26089|Observatory Hill Beds|36096|6|Mentioned|Fig.3|||||||||
26089|Observatory Hill Beds|36109|6|Mentioned|p68|||||||||
26089|Observatory Hill Beds|36110|6|Mentioned|p48|||||||||
26089|Observatory Hill Beds|36491|6|Mentioned|Fig.2|||||||||
26089|Observatory Hill Beds|36920|6|Mentioned|p167|||||||||
26089|Observatory Hill Beds|38022|6|Mentioned|Fig.4|||||||||
26089|Observatory Hill Beds|38157|6|Mentioned|Table VIII|||||||||
26089|Observatory Hill Beds|38329|3|Fully described|p197|||||||||
26089|Observatory Hill Beds|38604|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26089|Observatory Hill Beds|38605|5|Briefly described|Table 3|||||||||
26089|Observatory Hill Beds|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Early to Late Cambrian||||||
26089|Observatory Hill Beds|39762|6|Mentioned|p92|||||||||
26089|Observatory Hill Beds|39912|6|Mentioned|p7|||Locality plan||||||
26089|Observatory Hill Beds|40432|6|Mentioned|Fig.2|||||||||
26089|Observatory Hill Beds|40912|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
26089|Observatory Hill Beds|41103|6|Mentioned|p261|||||||||
26089|Observatory Hill Beds|41117|6|Mentioned|p446|||||||||
26089|Observatory Hill Beds|41276|6|Mentioned|Fig.1|||||||||
26089|Observatory Hill Beds|41609|5|Briefly described|Fig.5|||||||||
26089|Observatory Hill Beds|42356|5|Briefly described|Fiche 7 P15 Table 2|Cambrian||See also Microfiche 7 Fig.4, Fig.9||||||
26089|Observatory Hill Beds|42816|6|Mentioned|p14|||||||||
26089|Observatory Hill Beds|43048|6|Mentioned|p14|||||||||
26089|Observatory Hill Beds|43713|6|Mentioned|p2||Cambrian|||||||
26089|Observatory Hill Beds|45149|6|Mentioned|p43|||See also Table 1 and P15.||||||
26089|Observatory Hill Beds|46975|6|Mentioned|p89|||||||||
26089|Observatory Hill Beds|49792|5|Briefly described|Fig.5|||||||||
26089|Observatory Hill Beds|69648|6|Mentioned|p19|||A 594 m thick section in drillhole Wilkinson l on adjacent TALLARINGA was originally referred to as Observatory Hill Beds, but Brewer et al. (1987) correlated these sediments with Ouldburra Formation. See Observatory Hill Formation and Ouldburra Formation.||||||
26089|Observatory Hill Beds|69649|6|Mentioned|p58|Cambrian|Cambrian|Carbonate-bearing. Tested for phosphate.||||||
32547|Ochre Cove beds|44199|14|Not recorded|p595|||||||||
32547|Ochre Cove beds|44200|6|Mentioned|p.355|||||||||
41696|Olary 1590 Ma Supersuite|50605|5|Briefly described|p(ii), 1.3, 9.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1590Ma.||||||19-FEB-08
41697|Olary Pretectonic A-Type Suite|50605|5|Briefly described|p(i), 1.3, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1703-1700Ma.||||||07-NOV-08
41698|Olary Pretectonic I-Type suite|50605|5|Briefly described|p(iii), 11.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Age: 1629 +/- 12Ma (Shrimp).||||||07-NOV-08
36754|Older Granite Suite|23775|5|Briefly described|p721|Calymmian|Statherian|Age: 1690 -1400 Ma||||||22-SEP-09
36754|Older Granite Suite|23818|6|Mentioned|p36 Fig.9|Mesoproterozoic|Mesoproterozoic|||||||
36754|Older Granite Suite|67540|6|Mentioned|p37|||Of Coats and Blissett (1971). Included granites in the Mount Painter area which are now part of the Ninnerie Supersuite.||||||
36754|Older Granite Suite|69650|6|Mentioned|p3|||Coats and Blissettt, 1971. Granites in the Mount Painter area subsequently included in Ninnerie Supersuite.||||||
41699|Older Lincoln Supersuite|50605|6|Mentioned|p5.1|Paleoproterozoic|Paleoproterozoic|Superseded by Donington Granitoid Suite.||||||07-NOV-08
69134|Older Volcanic basalt|61135|6|Mentioned|p3|||informal name.||||||08-JUN-05
69134|Older Volcanic basalt|70998|14|Not recorded|p163|||Excursion details.||||||
29905|Olia Gneiss""|43052|6|Mentioned|p156|||In NT.||||||21-NOV-06
29905|Olia Gneiss""|61154|6|Mentioned|p7|||Informal name as mapped by Forman (1966b) - see Olia Gneiss - now reassigned as a granite of the Pitjantjatjara Supersuite.||||||
75372|Olia gneiss|64745|5|Briefly described|p372, p374 Tab. 1|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Mulga Park Domain, Musgrave Province. See Olia Gneiss.||||||18-SEP-09
42409|Olia-Alannah gneiss|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|See also Olia-Allanah Gneisses.||||||22-FEB-05
42410|Olia-Allanah Gneisses|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Massive to layered gneisses with local migmatite and granitoids.||||||22-FEB-05
39868|Olia-Allannah Gneisses|24497|5|Briefly described|Map legend||Mesoproterozoic|||||||
39867|Olla-Alannah gneiss|24497|6|Mentioned|Map legend|||Informal name - also misspelt .  See also Olia-Allannah Gneisses.||||||
29899|Olympic Dam Formation""|43052|5|Briefly described|p135|||||||||
78613|Olympic Dam Suite|65390|5|Briefly described|p27|Calymmian|Calymmian|Said to be of Budd et al. (1998) [NB: 'Roxby Downs type' used, not 'Olympic Dam Suite']. Strongly fractionated and oxidised granites of the Hiltaba Suite; related to Cu-Au systems on the eastern Gawler Craton.||||||
78613|Olympic Dam Suite|72459|5|Briefly described|p11, p39|Mesoproterozoic|Mesoproterozoic|Some samples exhibit a combination of low plagioclase and high k feldspar.||||||
72905|Olympic Dam breccia|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Informal name. Age:1590Ma. Geological Province: Gawler Craton (Olympic  Domain).||||||10-AUG-07
81384|Olympic Dam dolerite|70328|4|Described|p160,162-168|Tonian|Tonian|Geological province: Gawler Craton. Characterised by chilled margins, and most intensely altered along intrusive contacts with Roxby Downs Granite and Olympic Dam Breccia Complex. Magmatic apatite dated at 825+\-18 Ma (interpreted emplacement age; this study). U-Pb ages also include 821+\-15 Ma and 817+\-11 Ma (see p167). Geochemical and geochronological analysis suggests that the Olympic Dam dolerite is part of the Gairdner Dyke Swarm.|825+\-18 Ma|||Intrudes into Roxby Downs Granite and Olympic Dam Breccia Complex.|Suite of basaltic to doleritic dykes.|
78303|Ooddanatta Formation|68821|5|Briefly described|p296|Cretaceous|Cretaceous|Misspelt Oodnadatta Formation. Lower Cretaceous age.||||Unconformably overlain by the Eyre Formation.||
78302|Ooddnadatta Formation|68821|6|Mentioned|p292 Fig.1|||Misspelt Oodnadatta Formation.||Of the Rolling Downs Group.||||
77776|Oodnaminta Reef Complex|67180|5|Briefly described|p599, p609-12|Cryogenian|Cryogenian|Paleogeographic feature equivalent to the Balcanoona Formation. Regional exposure and erosion event (unconformity at base of Weetootla Dolomite Member and Yankaninna Formation) corresponds to the cessation of growth of this reef complex likely due to glacioeustatic processes or possibly a regional tectonic event.||||Unconformably overlain by the Weetootla Dolomite Member.||
77776|Oodnaminta Reef Complex|70021|5|Briefly described|p97-98, 100, 102-103, 105-109|Cryogenian|Cryogenian|Northern Adelaide Fold Belt. A series of prograding barrier reef systems. Deposition was synchronous with Tapley Hill Formation. Geochemistry of marine cements discussed in detail; related to oxic/anoxic seawater.|~650 Ma.|Balcanoona Formation.|||Almost entirely dolomite. Abundant microbialites and depositional micrites, initially deposited as aragonite, underwent dolomitization. Dolomite marine cements abundant throughout.|
40404|Ooldea Formation, lower|24606|6|Mentioned|p962|||Informal name. Geological Province: Eucla Basin||||||
40405|Ooldea Formation, upper|24606|6|Mentioned|p963|||Informal name. Geological Province: Eucla Basin||||||
72722|Ooldea Range barrier sands|62961|5|Briefly described|p15|Paleogene|Paleogene|In the eastern Great Victoria Desert.  Overlain by Quaternary longitudinal dunes.||||||07-NOV-08
38561|Ooldea Sand, "Lower"|24396|5|Briefly described|p222, p228|Late Eocene|Late Eocene|Informal name - Ooldea Sand.  Aeolian quartz sand.  See also p218 Fig.3.  Underlying unit: Khasta Formation.||||||
38562|Ooldea Sand, "Upper"|24396|5|Briefly described|p223, p228|Late Eocene|Late Eocene|Informal name - see Ooldea Sand.  See also p218 Fig.3.||||||
38724|Ooldea Sand, "lower"|24397|5|Briefly described|p240|||Informal subdivision of Ooldea Sand.  Interpreted as Ooldea Sand in the Ooldea Range.||||||
38726|Ooldea Sand, "upper"|24397|5|Briefly described|p240, p244|||Informal subdivision of Ooldea Sand.  Interpreted as Ooldea Sand in the Barton and Paling Ranges.  Geological Province: Eucla Basin.||||||
38560|Ooldea Sand, Lower|24396|5|Briefly described|p218 Fig.3, p222|Middle Eocene|Middle Eocene|Informal name - see Ooldea Sand.  See also p222 Fig. 5 and p228. Geological Province: Galwer Craton.||||||
38560|Ooldea Sand, Lower|24397|6|Mentioned|p236 Fig. 2|||||||||
38560|Ooldea Sand, Lower|24606|4|Described|p958 Fig. 3|Middle Eocene|Middle Eocene|Overlain by the upper Pidinga Formation. Overlies the Paling Limestone. Geological Province: Eucla Basin||||||
38560|Ooldea Sand, Lower|65194|6|Mentioned|p170|||Deposited as a barrier island complex.||||||
38563|Ooldea Sand, Upper|24396|5|Briefly described|p218 Fig.3, p223|Middle Eocene|Middle Eocene|Informal name - see Ooldea Sand.  See also p222 Fig. 5 and p228. Geological Province: Galwer Craton.||||||
38563|Ooldea Sand, Upper|24397|6|Mentioned|p236 Fig. 2|||||||||
38563|Ooldea Sand, Upper|24606|5|Briefly described|p958 Fig. 3|Late Eocene|Late Eocene|Geological Province: Eucla Basin||||||
38722|Ooldea Sand, lower|24397|6|Mentioned|p237|||Informal - see Ooldea  Sand.||||||
69636|Ooldea Sandstone|61155|5|Briefly described|p17|Late Eocene|Late Eocene|Overlies part of Hampton Sandstone. Age: 37.5-36.5Ma. Max. thickness: 50m. Geological Province: Eucla Basin.||||||
69636|Ooldea Sandstone|67789|6|Mentioned|p47|||Nullarbor Plain, Eucla Basin. Associated with the Eocene Ooldea Range. Reworked sediment of this unit forms middle Miocene beach ridges.||||||
81386|Ooldea sands|70397|5|Briefly described|p3|Middle Miocene|Middle Miocene|Eucla Basin. Note also late Eocene Ooldea dunes shown in same diagram.||Unit of Eucla Group.||||16-AUG-19
78614|Oorlana Metasomatite|65390|6|Mentioned|p18|Mesoproterozoic|Mesoproterozoic|Moonta Domain, Gawler Craton.||||||
22595|Oorlano Metasomatites|22629|6|Mentioned|p161|||||||||
37080|Oorlano Metasomite""|23719|6|Mentioned|p17|||Geological Province: Gawler Craton||||||
41701|Opal Fields Suite|50605|5|Briefly described|p8.3|||Of the Hiltaba Supersuite. Geological Province: Gawler Craton & Curnamona Province.||||||
41701|Opal Fields Suite|72459|5|Briefly described|p13|Mesoproterozoic|Mesoproterozoic|Sample initial Nd value is quoted by Creaser (1989).|||||Mafic granitoids.|
25368|Opaminda Siltstone|23818|5|Briefly described|p55|||Uppermost unit of the Upper Callanna Beds. Max. thickness: 1250 ft. Overlying unit: Wortupa Quartzite.||||||18-APR-05
25368|Opaminda Siltstone|34535|5|Briefly described|p55|||Top member. Upper Callanna Beds||||||
28895|Oraparina Shale|36198|6|Mentioned|Fig.I.2|||||||||
28895|Oraparina Shale|36525|6|Mentioned|Fig.5|||Misspelling of Oraparinna Shale?||||||
28895|Oraparina Shale|40856|5|Briefly described|p312|||Mention Fig.23.6||||||
67948|Oraparinna Shale, lower|44133|5|Briefly described|p3, 25|Botomian||Conformably overlies: Bunkers Sandstone, lower Mernmerna Formation.||||||
42529|Otway Group, Lower|23818|6|Mentioned|p150|||Geological Province: Otway Basin. Informal name - see Otway Group.||||||
69714|Otway Group, lower|23830|6|Mentioned|p2|Early Cretaceous|Late Jurassic|Informal - see Otway Group.  Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
69715|Otway Group, upper|23830|5|Briefly described|p2, p17|Early Cretaceous|Early Cretaceous|Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
69715|Otway Group, upper|24453|5|Briefly described|p809 Fig.2|Albian|Aptian|Informal. Of Otway Group. Geological Province: Otway Basin.||||||07-FEB-11
28897|Otway Supergroup|12781|6|Mentioned|p386|Early Cretaceous|Early Cretaceous||||Crayfish Group, Eumeralla Formation.|Overlies Casterton Formation.||
28897|Otway Supergroup|22674|5|Briefly described|Fig.2 p719, p729|Albian|Berriasian|||||||
28897|Otway Supergroup|22686|5|Briefly described|Fig3p745,746-49|Early Cretaceous|Early Cretaceous|Comprises Casterton Formation, Crayfish Group, Eumeralla Formation. Geological Province: Otway Basin.||||||17-JAN-06
28897|Otway Supergroup|22875|6|Mentioned|p14|||||||||
28897|Otway Supergroup|23792|5|Briefly described|p26|Albian|Berriasian|Geological Province: Otway Basin||||||
28897|Otway Supergroup|24113|5|Briefly described|p278|||Maximum Thickness: ~ 5km.  Geological Province: Otway Basin.||||||
28897|Otway Supergroup|24200|5|Briefly described|p409|Early Cretaceous|Late Jurassic|Geological Province: Otway Basin.  Mentioned in the context of the Otway Supergroup Equivalent.||||||
28897|Otway Supergroup|24314|5|Briefly described|p61 Fig.2|Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
28897|Otway Supergroup|24551|6|Mentioned|p245|||||||||
28897|Otway Supergroup|24562|4|Described|p4, 6, 8.|Early Cretaceous|Late Jurassic|Includes: Eumeralla Formation, Crayfish Group.  Geological Province: Otway Basin.||||||
28897|Otway Supergroup|42079|4|Described|p266|||See also Fig.2||||||
28897|Otway Supergroup|43171|4|Described|5|||||||||
28897|Otway Supergroup|43195|5|Briefly described|Map Legend||Early Cretaceous|See also commentary on back of map.||||||
28897|Otway Supergroup|43733|6|Mentioned|p37|||||||||
28897|Otway Supergroup|43744|6|Mentioned|Fig.3,p3|||||||||
28897|Otway Supergroup|44133|5|Briefly described|p142, 94 Fig. 9.2|Cretaceous|Cretaceous|Geological Province: Otway Basin.||||||
28897|Otway Supergroup|61045|6|Mentioned|p93|Early Cretaceous|Early Cretaceous|Geological Province: Otway Basin.||||||
28897|Otway Supergroup|61528|6|Mentioned|p823, p826|||||||||
28897|Otway Supergroup|61547|6|Mentioned|p461 Fig.2. |Albian|Berriasian||||Includes Crayfish Group.|Is overlain by Sherbrook Group.||
28897|Otway Supergroup|61622|5|Briefly described|p436 Fig. 2, p438 Fig. 4|Cretaceous|Cretaceous|Includes Winderemere Sandstone Member and Eumeralla Fromation. Geological Province: Otway Basin.||||||07-FEB-11
28897|Otway Supergroup|61627|5|Briefly described|p499, p501, p500 Fig. 2|Late Cretaceous|Early Cretaceous|Includes Crayfish Group and Eumeralla Formation. Geological Province: Otway Basin.||||||07-FEB-11
28897|Otway Supergroup|63122|5|Briefly described|p17 Fig. 4.3|Albian|Berriasian|Includes Eumeralla Formation and Crayfish Group units. Geological Province: Otway Basin. ||||||
28897|Otway Supergroup|63124|5|Briefly described|p49 Fig. 5.2|Early Cretaceous|Early Cretaceous|Includes Crayfish Group and Eumeralla Formation. Geological Province: Otway Basin.||||||
28897|Otway Supergroup|63125|6|Mentioned|p103|||Geological Province: Otway Basin||||||
28897|Otway Supergroup|63267|5|Briefly described|p485 Fig.2|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin.|||Crayfish Group, Eumeralla Formation.|Unconformably overlies Casterton Formation.||
28897|Otway Supergroup|63431|5|Briefly described|p677 Fig. 2|Albian|Berriasian|Includes the Crayfish Group and Eumeralla Formation. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
28897|Otway Supergroup|67366|6|Mentioned|p104. |Early Cretaceous|Early Cretaceous||||Includes Eumeralla Formation.|||
28897|Otway Supergroup|69651|6|Mentioned|p6|Early Cretaceous|Late Jurassic|Otway Basin. Includes Crayfish and Eumeralla Supersequences. Up to 8km thick; continental and fluvio-lacustrine sediments.||||||
28897|Otway Supergroup|72050|6|Mentioned|p233 Fig.2, 237|Early Cretaceous|Late Jurassic|||||||
28897|Otway Supergroup|73356|6|Mentioned|p1|||[Superseded by Otway Group]. See Lovibond et al. (1995) and Boult and Hibburt (2002).||||||
67949|Otway Supergroup, Lower|44133|5|Briefly described|p142|Mesozoic|Mesozoic|||||||
67950|Otway Supergroup, Upper|44133|5|Briefly described|p145|Mesozoic|Mesozoic|||||||
67951|Ouldburra Formation, lower|23981|6|Mentioned|p62-63, p77|Early Cambrian|Early Cambrian|Informal - see Ouldburra Formation. Geological Province: eastern Officer Basin.||||||
67951|Ouldburra Formation, lower|44133|6|Mentioned|p35|||||||||
67951|Ouldburra Formation, lower|62570|6|Mentioned|p581|Early Cambrian|Early Cambrian|Informal - see Ouldburra Formation. Cyclic suite of halite-carbonate-siliciclastic units.  ||||||
67952|Ouldburra Formation, upper|44133|5|Briefly described|p37|||Sabkha deposits. ||||||
80366|Outalpa Quartzites|70657|6|Mentioned|p22|||Campana and King (1958). Suggested in this study that the name be altered to Outalpa Quartzite Member, and applied to the lower part of the Tommie Wattie Formation.||||||
40361|Padathway Formation|23921|5|Briefly described|p1109 Table 2|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
75094|Padthaway Granite|64769|6|Mentioned|p28|Plaeoproterozoic|Paleoproterozoic|Dimension stone name.||||||21-APR-09
40667|Padthaway Ridge granites|23309|6|Mentioned|p48|||||||||
35823|Padthaway granite|23317|6|Mentioned|378|||||||||
28902|Painter Complex|30669|6|Mentioned|p303|||||||||
38565|Paling Limestone|24396|5|Briefly described|p218 Fig.3|Eocene|Eocene|[Misspelling of Paling Formation?].||||||19-JAN-15
38565|Paling Limestone|24606|4|Described|p958 Fig. 3|Middle Eocene|Middle Eocene|Overlain by the Lower Ooldea Sand. Overlies the lower Pidinga Formation. Geological Province: Eucla Basin||||||
38565|Paling Limestone|61856|5|Briefly described|p300 Fig.2, p311, p317 |Middle Eocene|Middle Eocene|Formerly Paling Member of Wilson Bluff Limestone.|||||A thin glauconitic and carbonaceous clayey and silty limestone.|19-FEB-15
38565|Paling Limestone|65891|6|Mentioned|p221 Fig.5. |Paleogene|Paleogene|East Eucla Basin. Age shown as Bartonian.||||||
33816|Paling Member|22587|6|Mentioned|p79 Fig.7|Late Eocene|Middle Eocene|||||||
33816|Paling Member|22613|5|Briefly described|p21|||||||||
33816|Paling Member|23488|5|Briefly described|p36, p38 Fig. 3|Middle Eocene|Middle Eocene|See also p39 Fig. 5.  Of the Wilson Bluff Limestone.  Marine limestone consisting of calcareous, carbonaceous and glauconitic sand with typical cool-water biota.  Geological Province: Eucla Basin.||||||
33816|Paling Member|24396|5|Briefly described|p222|Eocene|Eocene|Elevated to formation status by Clarke et al (2003) - see Paling Formation.  Unit lies between the upper and lower parts of the Pidinga Formation.  Formerly a member of the Wilson Bluff Limestone.||||||
33816|Paling Member|24397|5|Briefly described|p235, p238|||Upgraded to formation status - see Paling Formation.  Of Wilson Bluff Limestone.   Geological Province: Eucla Basin.||||||
33816|Paling Member|24606|5|Briefly described|p958 Fig. 3|Middle Eocene|Middle Eocene|Geological Province: Eucla Basin||||||
33816|Paling Member|24617|6|Mentioned|p115 Fig. 3|Eocene|Eocene|Nomenclature from previous work of Benbow 1993; Benbow et al. 1995 and Alley et al. 1999. Name may now be superseded. Geological Province: Eucla Basin.||||||15-APR-09
33816|Paling Member|44133|5|Briefly described|p153 Fig. 10.2|Late Eocene|Late Eocene|Geological Province: Eucla Basin. ||||||
33816|Paling Member|61856|6|Mentioned|p311|||Benbow et al. (1982). Subsequently Paling Formation.||Unit of Wilson Bluff Limestone.||||
33816|Paling Member|69648|4|Described|p23-25, map legend|||Eucla Basin. High energy limestone with distinctive grainy nature indicative of above wavebase, higher energy, nearshore environments. Type section: 16.7-28.4 m in Teitkins Well on OOLDEA (~12 m thick; lower and upper boundaries are clearly visible). Only known from this well. Stratigraphy of grainy limestones of Eocene age in basin are not well understood, hence Paling Member is included in Wilson Bluff Limestone. Occurrences north of Maralinga are likely correlatives of Toolinna Limestone (Lindsay and Harris, 1975). Proximal occurrences of Eocene limestone occur on west side of Eucla Basin, in tributary of Lefroy Palaeoriver, are namely Norseman Limestone (Gregory, 1916; Clarke, 1994).||Wilson Bluff Limestone||Is overlain conformably by Hampton Sandstone; at base, sharply overlies Pidinga Formation.|Predominantly very fine to fine grained calcarenite, or a bryozoan, echinoidal, grainstone; foraminifera relatively minor (1-2 %) but important; friable to moderately indurated.|
28904|Pandurra quartzite|31395|6|Mentioned|p64|||||||||
27278|Paney Rhyolite|24346|5|Briefly described|p102|||Now included as a member of the Eucarro Rhyolite - see Paney Rhyolite Member.||||||
27278|Paney Rhyolite|24474|5|Briefly described|p36 Fig. 1|||Of the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
27278|Paney Rhyolite|40430|2|Defined|p2|Mesoproterozoic|Mesoproterozoic|||||||
27278|Paney Rhyolite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
27278|Paney Rhyolite|42283|6|Mentioned|Fig.5 P82|||||||||
27278|Paney Rhyolite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
27278|Paney Rhyolite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
27278|Paney Rhyolite|43052|5|Briefly described|p111|||of Gawler Range Volcanics||||||
27278|Paney Rhyolite|65922|5|Briefly described|p17 Tb. 2, p19, p21|Calymmian|Calymmian|Of Gawler Range Volcanics. Brown, pink and green rhyolite grading to rhyodacite. Lavas, domes and ignimbrites. Overlies, and dykes within, the Yannabie Rhyodacite. Intrudes Eucarro Dacite.||||||
27278|Paney Rhyolite|67028|5|Briefly described|p362, p364 Tb.1|Calymmian|Calymmian|Information on magnetic characteristics presented. Described as Roxby Downs-type p362, but shown as Kokatha-type in Table 1.||Gawler Range Volcanics||||24-APR-12
27278|Paney Rhyolite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Fine- to coarse-grained, porphyritic dacite, commonly flow-banded; locally contains large lithic clasts.|
27278|Paney Rhyolite|72459|5|Briefly described|p17, p47|Mesoproterozoic|Mesoproterozoic|||Gawler Range Volcanics||||
38172|Paney Rhyolite""|24346|4|Described|p99, p101|||Now included as a member of Eucarro Rhyolite - see Paney Rhyolite Member.||||||
34587|Paning Sandstone Member|22839|6|Mentioned|P33|||||||||
83056|Panning Member|73167|6|Mentioned|p664 Fig. 2|Triassic|Triassic|Cooper Basin. Contains oil and gas.||Nappamerri Group||||
83056|Panning Member|73244|6|Mentioned|p86|Triassic|Triassic|[Possibly a misspelling of Paning Member]. Cooper Basin. Along with Callamurra Member, Wimma Sandstone Member and Tinchoo Formation, shown as floodplain, lacustrine, fluvial channels. Oil and gas identified.||||||
83056|Panning Member|73343|6|Mentioned|p337|Triassic|Triassic|Cooper Basin. Hosts oil and gas.||Nappamerri Group||Underlain by Callamurra Member. Overlain by Wimma Sandstone Member.||
83056|Panning Member|73479|5|Briefly described|p156 Fig.2, p159|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment.|ca 243 Ma|Nappamerri Group||Overlies Callamurra Member, underlies Wimma Sandstone Member||
67953|Pantapinna Sandstone, lower|44133|6|Mentioned|p30|||||||||
77405|Parabarana Formation|65376|6|Mentioned|p220 Fig.6.22.|Cretaceous|Cretaceous|||||||
39211|Parachillna Slate|23731|5|Briefly described|p27|||Of Tapley Hill Formation.||||||
39211|Parachillna Slate|64769|6|Mentioned|p27|||Dimension stone name.||||||06-MAY-09
67985|Parachilna Formation, upper|23981|6|Mentioned|p15|||Informal - see Parachilna Formation.||||||
67985|Parachilna Formation, upper|44133|6|Mentioned|p22|||||||||
72818|Parachilna formation|23981|6|Mentioned|p13|||Informal - see Parachilna Formation.||||||
39919|Parakeelya Alkaki Member|24112|5|Briefly described|p254 Fig.2|Early Cambrian|Neoproterozoic III|Geological Province: Officer Basin||||||
39919|Parakeelya Alkaki Member|72478|6|Mentioned|p8|Early Cambrian|Early Cambrian|Officer Basin. Shown as Parkeelya Alkali Member p69, Parakeelya Alkali Member Fig 7 p70.||Observatory Hill Formation||||29-MAR-21
34528|Paralana Gneiss|22795|5|Briefly described|p69|Mesoproterozoic|Proterozoic|||||||
74124|Paralana Granodiorite|62962|5|Briefly described|p2283 Fig. 1(c), p2285, p2284 Fig. 2,|Paleozoic|Paleozoic|Geological Province: Mount Painter Province. Age: 423+/-6Ma (K-Ar) and 432+/-1Ma (Ar/Ar). Epigranular, medium- or corse-grained granodiorite with plag, qtz, biotite and minor K-feld and hornblende.||||||07-FEB-11
74124|Paralana Granodiorite|67430|6|Mentioned|p38|||Informal name for Hodgkinson Granodiorite (see reference p39).||||||
74124|Paralana Granodiorite|68205|5|Briefly described|p85-86,88-96,98,100-102|Paleozoic|Paleozoic|Emplaced/intruded during an Orodvician tectonic event 440-460 Ma. Generally undeformed; calcic to calc-alkalic. Metaluminous in composition and related to British Empire Granite. Geochemical analysis provided from p88-92. Nd isotope analysis on p92-94. U-Pb zircon geochronology on p94-99. Exact age is poorly contrained, but broadly correable with U-Pb mozanite age of 441-445 Ma (from Wulser, 2009).|||||Granodiorite; quartz, plagioclase, K-feldspar, with biotite.|
82108|Paralana granodiorite|72459|5|Briefly described|p58, p67-70, p73, p90-93, p98, p100|Delamerian|Mesoproterozoic|Informal name of Neumann (1996) and Paul (1998). Mt Painter/Babbge inliers. Together with the Mudnawatana Tonalite, the Gordon Springs Granodiorite and the British Empire Granite forms so called group 3 of this study.Chemically very similar to the Mudnawatana Tonalite and the Gordon Springs Granodiorite and on that basis the authors group these 3 units together into the Paralana granodiorite. Dating via the Kober evaporation technique have failed to show whether this unit is Late Mesoproterozoic or Delamerian in age. Chemical characteristics are discussed.||||||
68969|Parara Limestone""|60418|6|Mentioned|p135|||||||||
72819|Parara Limestone, lower|23981|6|Mentioned|p59, p62|||Informal - see Parara Limestone.||||||
72820|Parara Limestone, middle|23981|6|Mentioned|p59|||Informal - see Parara Limestone.||||||
72821|Parara Limestone. upper|23981|6|Mentioned|p60|||Informal - see Parara Limestone.||||||
26832|Parara marine limestones|39352|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
39206|Parilla-Loxton Sands|23731|5|Briefly described|p22|Tertiary|Tertiary|Geological Province: Murray Basin.||||||
77510|Paring Member|62537|6|Mentioned|p191 Fig.2. |Middle Triassic|Middle Triassic|Cooper Basin.||Unit in Arrabury Formation.||||
39580|Paringa Andalusite Beds|24465|5|Briefly described|p346 fig.3|||Of Mirams, 1962 - of the Brukunga Formation.  Probably superseded.||||||19-JAN-05
41744|Pata limestone|50154|5|Briefly described|p135|||Informal name. Of the Murray Group.||||||
40094|Patchawarra Formation, lower|24210|6|Mentioned|p133|||Informal - see Patchawarra Formation.||||||
40077|Patchawarra Formation, upper|24210|6|Mentioned|p133|||Informal - see Patchawarra Formation.||||||
40077|Patchawarra Formation, upper|24212|6|Mentioned|p75|Early Permian|Early Permian|Informal name - see Patchwarra Formation. Geological Province: Cooper Basin.||||||
75369|Patchawarra Sandstone|63832|5|Briefly described|p131 fig 2|Cisuralian||Of Cooper Basin.|||||Alluvial facies (mudrocks, sandstones and conglomerates) and pyroclastic rocks underlie glacial deposits of C3. Laminated mudrocks, diamictites, siltstone clast breccias, interbedded with lesser siltstones, sandstones and conglomerates, of C4.|13-DEC-17
75369|Patchawarra Sandstone|64631|5|Briefly described|p44 Fig.2.|Artinskian|Sakmarian|Cooper Basin. Biostratigraphic age control for base and top.||||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
75369|Patchawarra Sandstone|65238|5|Briefly described|p3|||Geological province: Cooper Basin. Written as Patchawarra/Tirrawarra Sandstone.||||||17-FEB-10
82044|Patta Limestone Member|72445|6|Mentioned|App.7 p7, p20.|Miocene|Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991) as Pata Limestone and p20 as Patta Limestone.||Murray Group|||Includes limestone.|
78805|Paxton Granite Suite|64137|6|Mentioned|p1543 Fig.2 |||||||||
78804|Paxton Suite|63866|5|Briefly described|p6, p9, p17, p31|Statherian|Statherian|Wilgena Domain, Gawler Craton. |c. 1715 Ma (Budd and Fraser, 2004, Budd, 2006)|||||
78804|Paxton Suite|64137|6|Mentioned|p1542 Fig.1  |Paleoproterozoic|Paleoproterozoic|Very limited areal extent; restricted to Tarcoola goldfield area.||||||
78804|Paxton Suite|71318|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017964 (granite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1708+\-13 Ma; similar in age to the Paxton Granite (of Budd 2006) in the Tarcoola region.||||||
23896|Peela Conglomerate|23124|6|Mentioned|p397|||||||||
23896|Peela Conglomerate|39905|6|Mentioned|p4|||||||||
23896|Peela Conglomerate|60704|5|Briefly described|p687, p688 Fig.2|Paleoproterozoic|Paleoproterozoic|Base of Tarcoola Formation. Pink arkosic fluvial grit, with locally abundant banded-iron-formation fragments.||||||07-NOV-08
23896|Peela Conglomerate|63866|6|Mentioned|p9, p30|||||||||
23896|Peela Conglomerate|67058|5|Briefly described|p479.|Paleoproterozoic|Paleoproterozoic|Pebbles of BIF and quartzites are similar to those in the Mount Eba Formation.||Basal unit in Tarcoola Formation.||Is overlain by Fabian Quartzite.|Conglomerates, arkosic quartzites and green sandstones with pebbles of BIF and quartzites.|
77406|Pelican Formation|65376|6|Mentioned|p220 Fig.6.22.|Cretaceous|Cretaceous|||||||
30094|Pelite Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
30094|Pelite Suite|23248|5|Briefly described|Fig2p169|||||||||
30094|Pelite Suite|23869|5|Briefly described|p13|||Not a formal name.||||||
30094|Pelite Suite|24592|5|Briefly described|p635|||Of the Willyana Supergroup. Informal name. Interbedded pelite and psammite graphitic plus pyritic metasediments, amphibolite.||||||
30094|Pelite Suite|43086|5|Briefly described|p5|||||||||
30094|Pelite Suite|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Olary Domain. Informal name.||Unit in Willyama Supergroup.||Overlies Bimba Suite.||
30094|Pelite Suite|70657|5|Briefly described|p33. p42, p74, p77|||Clarke et al. (1986). Renamed the Strathearn Group by Conor (2000). Weathered Mn-rich zones form gossans.||Upper part of Willyama Supergroup.||||
69610|Peolpena Formation|61155|5|Briefly described|p17|Middle Eocene|Middle Eocene|May be misspelt? Age: 49.5-43Ma. Max. thickness: 180m. Geological Province: Polda Basin, Eyre Peninsula.||||||
25389|Pepagoona Porphyry|33472|6|Mentioned|p471|||||||||
25389|Pepagoona Porphyry|72459|6|Mentioned|p59, p78-81|Mesoproterozoic|Mesoproterozoic|||Mt Neill Suite||||
80470|Pepegoona "Porphyry"|71531|14|Not recorded|p9, 10, 11|||||||||
83031|Pepegoona Volcanics|73061|4|Described|p1067-1070, p1074 Fig.4, p1076-1077|Calymmian|Calymmian|Mount Painter Province. Oldest magmatic unit from field relationships, interpreted to be coeval with deposition of the Radium Creek Metamorphics. Deformed and metamorphosed to amphibolite facies before the intrusion of the Mount Neill Granite. Overlap in age with Mount Neill Granite interpreted as indicating they belong to the same magmatic event. Mean eHf value of +0.5 +/- 0.8. Crosscut by andesitic dyke (1571 +/- 5 Ma). Location in text includes p1072.|1596 +/- 6 Ma U-Pb LA-ICPMS zircon|||Interlayered with Radium Creek Metamorphics.|Felsic volcanics, porphyritic. Fine grained rhyolites and dacites with K-feldspar and quartz phenocrysts.|
26839|Pepogoona Porphyry|30176|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
70258|Pertatataka Formation, upper|61565|6|Mentioned|p616|||Informal name. Geological Province: Amadeus Basin||||||
70258|Pertatataka Formation, upper|61732|6|Mentioned|p168|||Informal - see Pertatakata Formation.||||||07-FEB-11
81692|Peryhumuck Calcalbitite|63102|6|Mentioned|p17|||Geological province: Olary Domain, Curnamona Province.  Superseded; see Peryhumuck Formation.||||||
82975|Peter Pan Suite|73235|6|Mentioned|p58-59|Statherian|Statherian|[Possibly a variation of Peter Pan Supersuite?].|1740-1700 Ma|||||
82109|Petermorra volcanics|72459|4|Described|p61-65, p70, p86, p94-99|Mesoproterozoic|Mesoproterozoic|Together with the Wattleowie granite, Terrapinna Granite, White Well Granite and the Golden Pole granite forms sub""group"" 2b of this report. Outcrops in the northern Mt Babbage inlier. Distinctive chemical features were not identified in this study.|1560 +/- 2 Ma (U-Pb zircon, Sheard et al., 1992)||||Porphyritic rhyolite, generally dark grey in colour, containing phenocrysts of K feldspar and some quartz.|
72822|Petrel Cove formation|23981|5|Briefly described|p13|Early Cambrian|Early Cambrian|Informal name. Of the Kanmantoo Group. Geological Province: Stansbury Basin (Fleurieu Peninsula).||||||
39241|Petrel Cove metasiltstones|23996|6|Mentioned|p354|||Formal name not intended -refers to rocks of the Petrel Cove Formation.  Geological Province: Adelaid Fold Belt.||||||07-MAR-05
38717|Pidinga Clay and Sands""|24397|5|Briefly described|p233|||Of Ludbrook, 1958.  Superseded by Pidinga Formation.  Geological Province: Eucla Basin.||||||
38717|Pidinga Clay and Sands""|65942|14|Not recorded|p75|||Passes laterally into the Hampton Sandstone.||||||
38517|Pidinga Formation, Lower|23488|5|Briefly described|p38 Fig. 3|||Informal name - see Pidinga Formation.  Geological Province: Eucla Basin.||||||
38517|Pidinga Formation, Lower|61630|6|Mentioned|p559|||Informal name, refers to the lower part of the Pidinga Formation.||||||
38516|Pidinga Formation, Upper|23488|5|Briefly described|p38 Fig. 3|Middle Eocene|Middle Eocene|Informal name - see Pidinga Formation.  Geological Province: Eucla Basin.||||||
38516|Pidinga Formation, Upper|24338|5|Briefly described|p947 Fig. 9|Early Eocene|Maastrichtian|Overlies the Potoroo Formation. Overlain by the Nullarbor Limestone. Geological Province: Ceduna Subbasin.||||||
38516|Pidinga Formation, Upper|24553|5|Briefly described|Figs. 8 and 10|Eocene|Paleocene|Geological Province: Duntroon Sub-basin.||||||07-FEB-11
38516|Pidinga Formation, Upper|61630|6|Mentioned|p556|||Informal name, refers to the upper part of the Pidinga Formation.||||||
38719|Pidinga Formation, lower|24397|5|Briefly described|p233|||Superseded by Maralinga Formation in South Australia, and by North Royal Formation in Western Australia.  Overlain by Paling Member.  Geological Province: Eucla Basin.||||||
38719|Pidinga Formation, lower|24606|4|Described|p958 Fig. 3|Middle Eocene|Middle Eocene|Informal - see Pidinga Formation. Overlain by the Paling Limestone. Geological Province: Eucla Basin. Formation is Fm in text.||||||
38718|Pidinga Formation, upper|24397|5|Briefly described|p240|||Informal name no longer required.  Overlain by Khasta Member.  Geological Province: Eucla Basin.||||||
38718|Pidinga Formation, upper|24606|4|Described|p958 Fig. 3|Late Eocene|Late Eocene|Informal - see Pidinga Formation. Overlain by the Khasta Formation. Overlies the Lower Ooldea Sand. Geological Province: Eucla Basin. Formation is Fm in text.||||||
34078|Pidinga Sands and Clays""|22613|3|Fully described|p19|Late Eocene|Middle Eocene|||||||
34227|Pidinga Sandstone|22663|6|Mentioned|S97-1 and 2 p3|||||||||
42430|Piginda Formation|24443|5|Briefly described|Fig.7|Eocene|Paleocene|Overlain by Nullabor Limestone and Wilson Bluff Liimestone. Geological Province: Bight Basin.||||||
42530|Pindinga Formation|23818|5|Briefly described|p194|Eocene|Eocene|Geological Province: Eucla Basin. Max. thickness: 86 ft.||||||
34950|Pindyan Sandstone|22900|6|Mentioned|83|||Misspelling of Pindyin Sandstone.||||||
34950|Pindyan Sandstone|61732|5|Briefly described|p58 Fig. 22|Cryogenian|Cryogenian|Geological Province: eastern Officer Basin.||||||07-FEB-11
35687|Pindyin beds|23288|6|Mentioned|p125||Neoproterozoic|of Major (1973). Superseded by Pindyin Sandstone.||||||14-OCT-08
35687|Pindyin beds|63397|6|Mentioned|5|Neoproterozoic|Neoproterozoic|||||||18-JUL-07
35687|Pindyin beds|65102|6|Mentioned|p365, p366 Fig. 4-41|Neoproterozoic|Neoproterozoic|Quarzitic and feldspathic sandstones. Correlated with Robert Formation, Townsend Formation of Officer Basin and Dean and Heavitree Quartzites of Amadeus Basin.||||||
35687|Pindyin beds|65410|6|Mentioned|p72.|Neoproterozoic|Neoproterozoic|Officer Basin. May be equivalent to Townsend Quartzite in the western Officer Basin. Part of Supersequence 2.||||||
68876|Pine Creek Kimberlite""|24584|6|Mentioned|p15|||Informal. See Pine Creek Kimberlite.||||||
68875|Pine Creek kimberlites|24584|5|Briefly described|p14|Jurassic|Jurassic|Informal. See Pine Creek Kimberlite. Geological Province: Ucocolla Inlier.||||||
74854|Piramimma Sand|64397|5|Briefly described|p232 Fig. 1A|Oilgocene|Oilgocene|Geological province: St Vincent Basin. Well-sorted, quartzose sand with indistinct cross-bedding and wood fragments. ||||||
67986|Piramimma Sand Member|44133|5|Briefly described|p165 Fig. 10.11|Middle Miocene|Early Oligocene|Geological Province: Saint Vincent Basin. Thickness: 50m. Of the Port Willunga Formation.||||||
33993|Pirramimma Sandstone|22525|3|Fully described|p35,37,39,40||Pleistocene|upgrading from Pirrammira Sand Member||||||
33993|Pirramimma Sandstone|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
33993|Pirramimma Sandstone|70660|5|Briefly described|p10-p11, p42|Early Pleistocene|Early Pleistocene|[Current name, supersedes the Pirramimma Sand and the Pirramimma Sand Member.]||||||
33993|Pirramimma Sandstone|72450|6|Mentioned|Brochure, Brochure map|Pleistocene|Pleistocene|Caps bedrock on hilltops and ridges in both the Noarlunga and Willunga Embayments. First identified in a water bore near Pirramimma, the sandstone is up to 100m thick. Exposed at Pirramimma, Wirra Wirra and Haselgrove and in the road cut on Main South Road, north of Aldinga.||||Unconformably overlies the Ochre Cove Formation. Underlies the Ngaltinga Formation.|Grey-white to yellow-buff, pebbly sandstone and silt.|
33993|Pirramimma Sandstone|73188|5|Briefly described|p319, p345-346|Pleistocene|Pleistocene|[Written as ""Pirramimma Sandstone"" and 'Pirramimma Sandstone']. Pliocene or Pleistocene. Mapped by Fairburn et al. (2010) in the Willunga Embayment; although, this name has precedence as an interpreted sandy member of the Port Willunga Formation in drill holes in the inland section of the Willunga Embayment (Cooper, 1979). Thus, the upper Cenozoic sandstones mapped with this name by Fairburn et al. (2010) are herein included in the Seaford Formation.||||Possibly equivalent to Seaford Formation.|Terrestrial sandstones.|
70566|Pitjantjatjara Suite|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Misspelt? - should be Pitjantjatjara Supersuite. Deformed granite. Geological Province: Musgrave Province.||||||
70566|Pitjantjatjara Suite|61864|6|Mentioned|p18 fig 4|||[Database says this is replaced by P. Supersuite]|||||Deformed granite.|
70566|Pitjantjatjara Suite|64745|6|Mentioned|p380 Fig.5|||Probable misspelling. See Pitjantjatjara Supersuite.||||||
70567|Pitjantjatjara Supersuite charnockites|61524|6|Mentioned|p17|||Informal reference to the charnockites of the Pitjanjatjara Supersuite. Geological Province: Musgrave Province.||||||26-MAY-09
75088|Plumbago formation""|23347|6|Mentioned|p54|||Of Conor (2000).  Dated from detrital zircons at 1.69Ga and younger.||||||
41702|Point Brown granodiorite|50605|5|Briefly described|p(i), 7.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Saint Peter Suite. Age: 1620-1619 +/- 15Ma (U-Pb).||||||07-NOV-08
80330|Point Ellen Limestone|70660|5|Briefly described|p29|Pleistocene|Pleistocene|Fossil assemblage briefly discussed. [Reference to Ludbrook (1973), should probably be Point Ellen Formation of Ludbrook (1983)]. Age controversial?||||Said by Ludbrook to be equivalent to the Burnham Limestone, but this now in doubt.|Highly fossiliferous limestone.|05-FEB-18
75584|Point Marsden Conglomerate|65624|5|Briefly described|map legend|Cambrian|Cambrian|Massive limestone with plentiful boulders containing Archaeocyathinae and a few gneiss, schist and red granite boulders at White Point and Point Marsden.||||||12-JAN-10
75582|Point Marsden Group|7992|4|Described|165|Late Cambrian|Early Cambrian|Includes Emu Bay Shales, Stokes Bay Sandstone, White Point Limestone. Name used interchangeably with Point Marsden beds.||||||12-JAN-10
75582|Point Marsden Group|65625|5|Briefly described|p123|||In part superseded by Kangaroo Island Group. Replaced Point Marsden series. Name dropped. Evidence of unconformity within Group. Of Sprigg (1955). All the rocks of Cambrian age which occur north of the Cygnet and Snelling Faults.||||||18-JAN-10
75583|Point Marsden beds|7992|4|Described|165, 166|Late Cambrian|Early Cambrian|Includes Emu Bay Shales, Stokes Bay Sandstone, White Point Limestone. Name used interchangeably with Point Marsden Group.||||||12-JAN-10
75585|Point Marsden conglomerates|65625|6|Mentioned|p123|||Informal reference to usage by Madigan (1928).||||||18-FEB-11
29472|Point Reynolds Formation|42966|6|Mentioned|p179|||||||||
35703|Policeman Well Sandstone""|23282|6|Mentioned|p83|||of Packham and Webby (1969), superceded by Blue Hills Sandstone.||||||
38631|Pondanna Dacite|24346|6|Mentioned|p104 Fig. 4|||Informal - Abbreviation of Pondanna Dacite Member.||||||
38631|Pondanna Dacite|65359|6|Mentioned|p17|Mesoproterozoic|Mesoproterozoic|Gawler Ranges. Mesoproterozoic. Extensive dacite lava flows: 10-60 km x 250 m thick (Allen et al. 2003), thought to have erupted at high temperatures from fissure vents in a continental setting.||||||
38631|Pondanna Dacite|68158|5|Briefly described|p4||||1592 +/- 3 Ma (U-Pb).|Gawler Range Volcanics.|||Massive, red, commonly columnar jointed dacite, porphyritic with phenocrysts of plagioclase, pyroxene; massive, black, grey or brown dacite, sometimes flow-banded, welded/chilled base of flow.|
38631|Pondanna Dacite|72065|6|Mentioned|p105-106, 108-110,112,115-116|||Geological province: Gawler Craton. Informal/Misspelt use: See Pondanna Dacite Member.||Unit of Yardea Dacite.||||10-JAN-20
81740|Poodla Hill Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||Olary Domain, Curnamona Province.|1719 +/- 3 Ma.|||Intrudes Wiperaminga Subgroup.||
81689|Poodla Hill Granite''|63102|5|Briefly described|p54|||Geological province: Olary Domain, Curnamona Province. Shows pervasive and fracture-controlled albitisation (+\-actinolite, titanite).||||||
34864|Poodla Hill Granodiorite|22965|6|Mentioned|p14||Statherian|||||||
34864|Poodla Hill Granodiorite|63866|6|Mentioned|p41|||Age derived from Page et al (in prep).|1719 +/- 3 Ma||||I type granodiorite.|
73189|Poodla Hill Suite""|63224|6|Mentioned|p12|||Geological Province: Curnamona Province. I-type granite. Although used on this map, recent work suggests that these polygons should be separated into time-equivalents of the older Lady Louise and Basso Suites.||||||09-SEP-13
81690|Poodla Hill Suite''|63102|5|Briefly described|p40,53|Statherian|Statherian|Geological province: Olary Domain, Curnamona Province. Magnetite-bearing granitoids, and are considered to have I-type affinities. Has a U-Pb zircon age of 1629+\-12 Ma for a body at Poodla Hill (Cook et al 1994), and 1641+\-11 Ma from a body proximal to that. LA ages by Freeman (1995) returns zircon age of 1681.8+\-10.1 Ma, approximating that of Lady Louise Suite. Undergone variable alkali and calc-silicate alteration.|||||Altered relatively mafic I-type granitoids, of granodiorite and monzogranite composition.|22-OCT-19
82110|Poodla Hill granodiorite|70658|6|Mentioned|p32|||Curnamona Province. Presented as Poodla Hill meta-granodiorite.||Basso Suite.|||I-type.|
82110|Poodla Hill granodiorite|72459|6|Mentioned|p107|Mesoproterozoic|Palaeoproterozoic|Olary Domain.|1629 +/- 29 Ma (Fanning, 1995)|||||
41703|Poodla Hill mafic granitoid|50605|5|Briefly described|p(iii)|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary I-Type suite.|1629 +/-12 (Cook et al 1994)|||||09-SEP-13
72283|Poodla granite|62514|6|Mentioned|p759 Fig. 13|||Informal - see Poodla Granite.  The name Poodla Hill is used in one figure - possibly name is incorrect?||||||16-SEP-09
81688|Poodla granite''|63102|6|Mentioned|p40|||Geological province: Olary Domain, Curnamona Province. See Poodla Hill Suite.||||||
83531|Poolalie Dolomite|73525|5|Briefly described|p19 Fig.13|||Cleve Domain.||Darke Peak Group|||Carbonates.|
78472|Poondanna Dacite Member|65922|6|Mentioned|p21|||Of Yardea Dacite. [Misspelling of Pondanna Dacite Member]||||||07-NOV-13
70340|Pooraka Formation Conglomerate I|62096|5|Briefly described|p288, p290 Fig. 3a|||Overlies the basal breccia of the Pooraka Formation.  Dark red weathered, poorly sorted coarse fluvial conglomerate with a sandy matrix.  Underlies Pooraka Formation Conglomerate II.  Also written as Pooraka Formation conglomerate I.||||||09-MAY-06
70341|Pooraka Formation Conglomerate II|62096|5|Briefly described|p288, p290 Fig. 3a|||Informal name for the conglomerate portion of the Pooraka Formation which overlies the Pooraka Formation Conglomerate I. Dark-brown weathered, carbonate-rich conglomerate. Also written as Pooraka Formation conglomerate II.||||||09-MAY-06
70339|Pooraka Formation colluvium|62096|6|Mentioned|p289|||Informal reference to a part of the Pooraka Formation.||||||
70342|Pooraka Formation talus breccia|62096|5|Briefly described|p288, p290 Fig. 3a|||Refers to the basal breccia of the Pooraka Formation.  Overlain by Pooraka Formation Conglomerate I.||||||09-MAY-06
25408|Pooraka Soil|30752|6|Mentioned|p6|||||||||
38524|Pooraka gravels|24176|6|Mentioned|p20|Tertiary|Tertiary|Informal name.||||||
38524|Pooraka gravels|62096|5|Briefly described|p291 Fig. 3i|||Variously termed Pooraka Formation river gravels, P.F. gravels II, P.F. gravels IV, P.F. river gravels V - all informal names for parts of the Pooraka Formation.||||||09-MAY-06
69612|Port Addis Limestone|61155|5|Briefly described|p18|Early Miocene|Late Oligocene|Misspelt - place name is Point Addis. Of the Torquay Group. Overlies Angahook Member (Demons Bluff Formation). Overlain by Puebla Formation. ||||||
68877|Port Campbell Formation|60421|5|Briefly described|p417, 418 Fig. 5|Miocene|Oligocene|Of the Heytsbury Group.||||||
76011|Port Elliot Shale|50133|6|Mentioned|p11 Tb.2|||Informal?||||||
83697|Port Elliot-Victor Harbor granite|73430|6|Mentioned|p517|Cambrian|Cambrian|S-type granite. Written as Pt Elliot -Victor Harbor granite.|508+/-2 Ma|||||
25409|Port Julia Greensand (Member)|33330|2|Defined|p164|late Eocene|late Eocene|||||||
69131|Port Julia Greensland Member|61121|5|Briefly described|Map legend|Eocene|Eocene|Name probably misspelt? Massive glauconitic, silty quartz sandstone with numerous bivalves, gastropods, corals, foramifera and bryozoans. Geological Province: St. Vincent Basin.||||||23-DEC-09
39958|Port Stanvac Sandstone Member|24195|1|Redefined|p43 Fig.2, p44|Neoproterozoic|Neoproterozoic|Definition included in article. Correlatives include Bayley Range Siltstone Member and Corraberra Sandstone Member. Parent: Brachina Formation. Overlying Unit: ABC Range Quartzite. Underlying Unit: Moorillah Siltstone Member. Max Thickness: 115m||||||
39958|Port Stanvac Sandstone Member|72450|5|Briefly described|Brochure map||||||||Laminated and cross-bedded red sandstone.|
39204|Port cambell Limestone|23768|5|Briefly described|p30 Fig.6|||Misspelt - see Port Campbell Limestone.||||||
73765|Potree Carbonate Member|63460|5|Briefly described|p847|Early Miocene|Early Miocene|Misspelt in text but correct in Fig. 3 (840).||||||05-FEB-08
42423|Pottyu Suite|24496|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Age: 1190-1140 Ma. Graniotoids. Some may be granitisation of Olia and Allanah Gneisses. Equivalent to Kultpittaja Granite COpmlex. Geological Province: Musgrave Block.||||||04-FEB-05
68970|Pound Group|60418|6|Mentioned|p134 Fig.1|Neoproterozoic|Neoproterozoic|||||||
68970|Pound Group|62784|5|Briefly described|p8 Fig.1|Neoproterozoic|Neoproterozoic|Includes Bonney Sandstone. Overlies Neoproterozoic Wilpena Group.||||Is overlain by Hawker Group.||20-MAR-12
68970|Pound Group|63569|6|Mentioned|p118 Fig. 2|Neoproterozoic|Neoproterozoic||||Includes Bonney Sandstone.|||
68970|Pound Group|65410|6|Mentioned|p74.|||Adelaide Geosyncline. Part of Supersequence 4.||||||
72906|Poverty Corner metasediments|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Informal name. Age: 1702+/-12Ma. Geological Province: Gawler Craton (Coulta Domain).||||||07-NOV-08
40088|Pretty Hill Formation shales|24209|6|Mentioned|p152|||Informal - see Pretty Hill Formation.||||||
28939|Pretty Hill Group|41185|6|Mentioned|Fig.13|||||||||
28939|Pretty Hill Group|65718|6|Mentioned|p11|||Otway Basin.||||||
76884|Pretty Hill Sandstone Member|61547|6|Mentioned|p461. |||Shown in Fig 2 as at base of Pretty Hill Formation, but described as 'main target reservoir at the top of the sequence'.||Unit in Pretty Hill Formation.||||
73538|Pretty Hill shale|63125|6|Mentioned|p107|||Not intended as a formal name - refers to shale within the Pretty Hill Formation called intra-Pretty Hill shale. Geological Province: Otway Basin||||||
28940|Pretty Hills formation|29523|6|Mentioned|p23|||||||||
78761|Pualco Formation|62085|6|Mentioned|p20 fig 5|Cryogenian|Cryogenian|||Umberatana Group||Is overlain by Holowilena Ironstone.|Diamictite.|
78761|Pualco Formation|65892|5|Briefly described|p33 Fig.18.|Cryogenian|Cryogenian|||Unit in Umberatana Group.||Is overlain by Holowilena Ironstone.||
78761|Pualco Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Yudnamutana Subgroup.||||
39957|Purple Series|24195|5|Briefly described|p42,43|Cambrian|Late Precambrian|Underlying Unit: Brighton Limestone||||||
40452|Quartzo-feldspathic Suite|24592|5|Briefly described|p635|||Informal name. Of the Willyama Supergroup. Overlain by the Calc-silicate Suite. Quartz albite +/- magnetic albitic siltstone/shale + magnetic and iron formation that is between this unit and the overlying Calc-silicate Suite.||||||
40452|Quartzo-feldspathic Suite|66857|5|Briefly described|pp971-972, p976.|Paleoproterozoic|Paleoproterozoic|Informal name for rocks in the Olary Domain, including widespread leucocratic quartzo-feldspathic gneisses formed from granitoids and co-magmatic felsic (rhyolitic) volcanics and epiclastic sediments. |c.1700 Ma (Ashley et al. 1997).|Unit in Willyama Supergroup.||||
30091|Quartzofeldspathic Suite|22575|5|Briefly described|p179 Fig.2|||of the Olary Block||||||
30091|Quartzofeldspathic Suite|23248|5|Briefly described|Fig2p169, 174, 179||Statherian|Max Age: 1699 (+/-) 10 Ma.||||||
30091|Quartzofeldspathic Suite|23869|5|Briefly described|p13|||Not a formal name.||||||
30091|Quartzofeldspathic Suite|43086|5|Briefly described|p2|||Not to be viewed as a strict stratigraphic unit.||||||
30091|Quartzofeldspathic Suite|64944|6|Mentioned|p27|Paleoproterozoic|Paleoproterozoic|Informal name of Clarke et al (1986) essentially equivalent to the Wiperaminga Subgroup (lower Curnamona Group). Written as "Quartzofeldspathic Suite"||||||07-FEB-11
30091|Quartzofeldspathic Suite|70657|6|Mentioned|p18, p77|||Clarke et al. (1986). Correlated with what is now the George Mine Formation. Appears on p77 to be part-equivalent to Curnamona Group.||||||
41704|Radium Creek granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Age: 1560Ma.||||||07-FEB-11
41704|Radium Creek granite|50605|5|Briefly described|p(ii), 1.4, 10.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Of the Moolawatana Suite. Age: ~1560Ma.||||||27-NOV-06
82038|Radium Hill breccia|67127|6|Mentioned|p113|||In the Mount Painter Complex. Curnamona Province, South Australia.|||||Hematitic breccia containing base-metal sulphides,uraninite, monazite, chlorite, carbonate, fluorite, quartz, and magnetite.|10-NOV-20
30518|Radium Ridge beds|43201|5|Briefly described|p13|||Variation on defined name Radium Ridge Breccia? Mount Painter Inlier.||||||
40461|Radium Ridge breccias|24593|6|Mentioned|p627|||Informal name.||||||
40461|Radium Ridge breccias|64329|5|Briefly described|P18|||Informal name. Occur in the Mount Painter Complex and Palaeozoic granitoids of the area, and consist of clasts of granitoid and metamorphic rocks with some massive hematitic breccia.||||||
75105|Ramco Limestone|64769|6|Mentioned|p28|Pliocene|Pliocene|Dimension stone name in South Australia.||||||21-APR-09
72882|Ramsay Limestone, lower|23981|6|Mentioned|p40|||Informal - see Ramsay Limestone.||||||
72881|Ramsay limestone|23981|6|Mentioned|p23|||Informal - see Ramsay Limestone; used interchangeably with the formal name.||||||
81694|Rasp Ridge Granite|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province. Also referred to as Rasp Ridge Gneiss on p40. See Rasp Ridge Granite Gneiss.|1682+\-3 Ma|||Intrudes Thackaringa Group.||
81694|Rasp Ridge Granite|72461|6|Mentioned|p6, p16||||1683 +/- 3 Ma|||||
80306|Rawlinna member|71361|5|Briefly described|p20, p27, |Miocene|Miocene|Eucla Basin. Informal name. Fossil assemblage described (p34-p35). See also p34-p35, p43, p119, p123, p141-p142.||Nullarbor Limestone||Overlies the Mullamullang Limestone Member.||31-JAN-18
81387|Rawlinna member''|70397|4|Described|p3-5,8-11,14|Middle Miocene|Middle Miocene|Eucla Basin. Proposed name for the unnamed upper unit of Nullabor Limestone overlying the basal Mullamullang Member. Depositional environment: wide, open shelf with effective circulation, normal marine salinity, and around 30-45 m water depth (Lowry, 1970). Comprises of Articulated Coralline Algae Facies, Benthic Foraminifera Facies, Echinoid Facies, and Planktonic Foraminifera Facies of the Nullabor Limestone.||Unit of Nullabor Limestone.||Underlain by/interbedded with Mullamullang Member.|Mudstone to rudstone and fossils include diverse benthic foraminifera, coralline algae, echinoids, bivalves, gastropods, planktonic foraminifera, serpulids and scleractinian corals.|
79556|Rawnsley Formation|67870|5|Briefly described|p9|Ediacaran|Ediacaran|Adelaide Rift System.||Pound Subgroup.||||
81234|Rawnsley Quartzite, upper|68030|5|Briefly described|p239,241|Cambrian|Ediacaran|Flinders Ranges. Comprises similar crossbedded, petee sandstones as those of the Chace Quartzite Member.||||Underlain by Ediacara Member.||
28954|Rawnsley Sandstone Member|33658|6|Mentioned|p171|||Fauna.||||||
67987|Reaphook Limestone""|44133|6|Mentioned|p24|||Of Gehling, 1971.||||||
75818|Red Banks charnockite|65485|6|Mentioned|p42, p41 Fig. 1|||Contains 2000 Ma metamorphic zircons. Shown as Red Banks Charnockite in Fig. 1. Geol. Prov: Gawler Craton.||||||
72789|Red Beds, Lower|63056|5|Briefly described|p81 Fig. 2|Middle Ordovician|Middle Ordovician|Probably an informal name referring to part of the Innamincka Formation.||||||
42339|Redbanks charnockite|60534|5|Briefly described|p572|Paleoproterozoic|Paleoproterozoic|Age: ca. 1715 Ma (Fanning, 1997). Geological Province: Gawler Craton.||||||07-NOV-08
68786|Reedy Creek Diorite|24509|6|Mentioned|p39 Fig. 1, p40|||Diorite dyke. See also p42. Geological Province: Murray Basin.||||||28-APR-05
68786|Reedy Creek Diorite|61307|5|Briefly described|p14 Fig. 6, p26|Ordovician||Older I-type suite which, geochemically, includes in part the Reedy Creek Granodiorite; this unit also forms part of the younger A-type suite. Age: 487+/-2Ma. Intrusive.||||||
39238|Reedy Creek Granite|23996|5|Briefly described|p362|||Geological Province: Adelaide Fold Belt.||||||28-APR-05
41465|Reedy Creek Tonalite|50437|6|Mentioned|p5.2|||Geological Province: Kimberley Region. Of the Dougalls Suite. Used interchangeably with Reedy Creek Granodiorite.||||||10-AUG-04
35821|Reedy Creek granodiorite|23317|6|Mentioned|378|||||||||
35821|Reedy Creek granodiorite|73430|6|Mentioned|p517|Cambrian|Cambrian|Has a tectonic fabric inferred to be D3.|492.6+/-1 Ma|||||
74105|Regional Suite|24197|4|Described|p32|Mesoproterozoic|Mesoproterozoic|Example of the Hiltaba Association. Includes the Triangle Hill granite. Age: ~1590Ma. Geological Province: Olary Domain.||||||07-FEB-11
41705|Regional suite|50605|5|Briefly described|p1.4, 9.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Of the Olary 1590 Ma Supersuite. Age: 1568.3 +/- 2.1Ma (U-Pb).||||||19-FEB-08
82045|Renmark Beds, Lower|72445|5|Briefly described|App.7 p20.|Paleocene|Paleocene|Apparently replaced by Warina Sand. Spelt as 'Lower Renmark Beds' in text.||||Shown as underlying Olney Formation.||
40363|Renmark beds, Lower|23921|5|Briefly described|p1109 Table 1|Eocene|Eocene|Geological Province: Murray Basin.  Informal-see Renmark Group||||||
40365|Renmark beds, Middle|23921|5|Briefly described|p1109 Table 1|Oligocene|Oligocene|Geological Provincve: Murray Basin.  Informal-see Renmark Group.||||||
39178|Renowden Metabasalt|24475|6|Mentioned|p55|||Redefined as Renowden Metabasalt Member of Matta Formation.||||||
73755|Renownden Metabasalt|63398|5|Briefly described|p669|Paleoproterozoic|Paleoproterozoic|Age: ca 1750Ma. Mafic rocks. ||||||07-NOV-08
73756|Renownden metabasalt|63398|6|Mentioned|p670 Fig. 6d|||Informal - see Renownden Metabasalt. ||||||
27549|Reynella Siltstone|32724|6|Mentioned|Fig.1|||Marinoan. Correlation||||||
27549|Reynella Siltstone|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
27549|Reynella Siltstone|33474|6|Mentioned|Fig.2|||||||||
27549|Reynella Siltstone|35255|5|Briefly described|p10|||See also Fig.6.||||||
27549|Reynella Siltstone|35678|6|Mentioned|p67|||Summary geological logs.||||||
27549|Reynella Siltstone|40456|4|Described|p21|||||||||
27549|Reynella Siltstone|40852|6|Mentioned|Fig.3.2|||||||||
27549|Reynella Siltstone|41581|5|Briefly described|p123|||||||||
27549|Reynella Siltstone|42239|6|Mentioned|p149|||||||||
27549|Reynella Siltstone|42338|5|Briefly described|p152|||||||||
27549|Reynella Siltstone|42410|6|Mentioned|p3|||||||||
27549|Reynella Siltstone|42522|4|Described|p162|Neoproterozoic||||||||
27549|Reynella Siltstone|42600|6|Mentioned|Fig.2 p4|||||||||
27549|Reynella Siltstone|42652|5|Briefly described|Fig. 3-11 P62|||||||||
27549|Reynella Siltstone|68241|6|Mentioned|p20 Fig.1|||||||||
39678|Rischbieth complex|24175|6|Mentioned|p48|||Informal name.||||||
26872|River Broughton Beds|22889|6|Mentioned|p35|Adelaidean|Adelaidean|Parent - Callanna Group.  Geological Province - Spalding Inlier.||||||
26872|River Broughton Beds|22926|6|Mentioned|37|||Geol Province Spalding Inlier. Parent Curdimurka Subgroup||||||
26872|River Broughton Beds|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Arkaroola Subgroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
26872|River Broughton Beds|32725|4|Described|p7|||New name proposed. Type section given.||||||
26872|River Broughton Beds|35328|6|Mentioned|Fig.1|||||||||
26872|River Broughton Beds|36733|6|Mentioned|Table 5|||||||||
26872|River Broughton Beds|37461|5|Briefly described|p335|||See also Table 5.I||||||
26872|River Broughton Beds|37854|6|Mentioned|Table 1|||||||||
26872|River Broughton Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
26872|River Broughton Beds|40294|6|Mentioned|p8|||||||||
26872|River Broughton Beds|41403|6|Mentioned|p51|||||||||
26872|River Broughton Beds|41404|6|Mentioned|p73|||||||||
26872|River Broughton Beds|42222|5|Briefly described|p12|||||||||
26872|River Broughton Beds|42223|5|Briefly described|p34|||||||||
26872|River Broughton Beds|42235|6|Mentioned|p134|||of Callanna Group. Overlain by Rhynie Sandstone (Emeroo Subgroup)||||||
26872|River Broughton Beds|43052|5|Briefly described|p175, p198 Table 6.1|||||||||12-MAR-14
26872|River Broughton Beds|43742|6|Mentioned|p37|||||||||
26872|River Broughton Beds|64796|5|Briefly described|p188 Fig.6, p192, p194 Tb.2 |Neoproterozoic|Neoproterozoic|See also p200 Fig.10, p202. Southern Flinders Ranges. Probably represents a part of the Curdimurka Subgroup.||||||
26872|River Broughton Beds|73188|6|Mentioned|p354|||Willouran age. Complexly folded and brecciated.||||Disconformably[?] overlain by Burra Group.||
25444|River Wakefield Subgroup|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
25444|River Wakefield Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Torrensian|Torrensian|Of the Burra Group. ||||||
25444|River Wakefield Subgroup|22869|6|Mentioned|P44, Table2|||||||||
25444|River Wakefield Subgroup|22889|5|Briefly described|p31|Adelaidean|Adelaidean|The River Wakefield Subgroup is down graded to formation status - details outlined on p33. Redefined River Wakefield Formation outlined on p38.||||||
25444|River Wakefield Subgroup|23054|6|Mentioned|p11|||||||||
25444|River Wakefield Subgroup|23314|5|Briefly described|331 Fig.2|||||||||
25444|River Wakefield Subgroup|24175|6|Mentioned|p11|||Of the BURRA region.||||||
25444|River Wakefield Subgroup|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Of Burra Group. Overlies Opaminda Formation. Overlain by Wortupa Quartzite. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
25444|River Wakefield Subgroup|35328|6|Mentioned|p11|||Previously River Wakefield Group||||||
25444|River Wakefield Subgroup|36733|6|Mentioned|p23|||See also P39.||||||
25444|River Wakefield Subgroup|37461|4|Described|p337|||||||||
25444|River Wakefield Subgroup|37854|6|Mentioned|p13|||||||||
25444|River Wakefield Subgroup|38157|6|Mentioned|Table III|||||||||
25444|River Wakefield Subgroup|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25444|River Wakefield Subgroup|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25444|River Wakefield Subgroup|39352|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25444|River Wakefield Subgroup|40225|6|Mentioned|Map sheet|||||||||
25444|River Wakefield Subgroup|40294|3|Fully described|p34|||||||||
25444|River Wakefield Subgroup|41401|6|Mentioned|Table 4|||||||||
25444|River Wakefield Subgroup|41404|4|Described|p92|||||||||
25444|River Wakefield Subgroup|41526|6|Mentioned|p32|||||||||
25444|River Wakefield Subgroup|42167|6|Mentioned|Fig.2 P115|||||||||
25444|River Wakefield Subgroup|42222|4|Described|p13|||||||||
25444|River Wakefield Subgroup|42238|6|Mentioned|Table 1 P75|||||||||
25444|River Wakefield Subgroup|43052|5|Briefly described|p177,Table 6.1|||of Burra Group||||||
25444|River Wakefield Subgroup|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Burra Group.||||||
25444|River Wakefield Subgroup|64793|6|Mentioned|p284 fig 3, p285 fig 4|||Adelaide Rift Complex.||Burra Group.||||
25444|River Wakefield Subgroup|64796|6|Mentioned|p191 Fig.9, p192|Neoproterozoic|Neoproterozoic|Carbonate deposition indicates lagonal to marginal marine environment.|||Includes Benbournie Dolomite, Stradbrooke Formation, Ingomar Quartzite, Boconnoc Formation, Blyth Dolomite Beds.|||
33343|River Wakefield group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Willouran.||||||
33343|River Wakefield group|71237|14|Not recorded|p9|||||||||
33343|River Wakefield group|71240|14|Not recorded|p6|||||||||
24474|Rockwater Beds|23054|5|Briefly described|p11|||||||||
24474|Rockwater Beds|24175|6|Mentioned|p9|||Geological Province: Peake and Denison Inliers.||||||
24474|Rockwater Beds|36733|2|Defined|p69|early Adelaidean|early Adelaidean|See also P31.||||||
24474|Rockwater Beds|37854|6|Mentioned|Table 1|||||||||
24474|Rockwater Beds|38108|6|Mentioned|Table 1|||||||||
24474|Rockwater Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24474|Rockwater Beds|40294|6|Mentioned|Table 2|||||||||
24474|Rockwater Beds|41403|4|Described|p66|||||||||
24474|Rockwater Beds|42238|6|Mentioned|p72|||||||||
24474|Rockwater Beds|43052|5|Briefly described|p175,Table 6.2|||of Curdimurka Subgroup.||||||
24474|Rockwater Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24474|Rockwater Beds|64796|6|Mentioned|p189 Fig.7, p195 Tb.3, p200 Fig.10, p202|Neoproterozoic|Neoproterozoic|Peake and Denison Ranges.||Unit in Callanna Group.||||
24474|Rockwater Beds|64797|6|Mentioned|p160 Fig.8|||||Callanna Group.||||
79557|Rook Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Curdimurka Subgroup.||||
41706|Roopena tuff|50605|5|Briefly described|p(ii), 8.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Lower Gawler Range Volcanics. Age: 1587 +/- 15Ma (U-Pb).||||||
82973|Roxby Down Granite|73256|6|Mentioned|p573|||[Probably a misspelling of Roxby Downs Granite].||Hiltaba Suite||||
75768|Roxby Downs granite|65455|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|This A-type-like granite is associated with the giant IOCG-U Olympic Dam deposit.||Of the Hiltaba Suite.||||09-MAY-12
41707|Roxby Downs suite|50605|5|Briefly described|p(ii), 1.3, 8.2, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Hiltaba Supersuite.||||||
81742|Roxby Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Southern Gawler Craton.|1588 +/- 4 Ma.|||||
83484|Royston Head Granite|73493|6|Mentioned|p732|||See also Royston Granite p718 Fig.5.||||||
83482|Royston Head mafic dykes|73493|5|Briefly described|p718-720, p722 Fig.9, p723 Fig.10|Calymmian|Calymmian|Subdivision of Daly Head Metadolerite, geochemistry is comparable to Southern Yorke peninsula mafic dykes. Depleted mantle model ages are mostly ca 2.9-2.5 Ga. See also p725 Fig.12. Also written as 'Roystone Head mafic dykes', and as Royton Head mafic dykes p718, Royston Head gabbro p719, p723 Fig.10.|ca 1564 Ma|Daly Head Metadolerite|||Gabbroic, tholeiitic.|
69614|Ruwarung member|61155|5|Briefly described|p3, p17|||Misspelt - see Ruwarung Member. Of the Port Willunga Formation. Geological Province: St Vincent Basin.||||||
34070|Saint Peter Suite|50605|5|Briefly described|p(i), 1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton and Curnamona Province. Age: 1630-1620Ma.||||||04-JUN-09
34070|Saint Peter Suite|71129|6|Mentioned|p14,17-18|Statherian|Statherian|Geological Province: Nuyts Domain, Gawler Craton. Moderately juvenile, bimodal magmatism.|c. 1640-1610 Ma|||||
34070|Saint Peter Suite|71318|5|Briefly described|p3,28|Paleoproterozoic|Paleoproterozoic|Geological province: Gawler Craton. Sample GSSA 2017965 (medium-grained granite) yielded an interpreted (weighted mean 207Pb/206Pb age) magmatic crystallisation age of 1725+\-19 Ma, with inherited zircon populations at c. 2310 Ma and 1725+\-19 Ma.||||||
34070|Saint Peter Suite|72237|6|Mentioned|p30|Paleoproterozoic|Paleoproterozoic||c. 1635-1605 Ma|||||
34070|Saint Peter Suite|72242|6|Mentioned|p27|Calymmian|Statherian|Geological province: Coompana Province, Western Gawler Craton. Bimodal magmatism associated with Kararan Orogeny.||||||
35884|Saltbush Subgroup|23347|2|Defined|p51 Tb. 1, p53 Fig. 3, p54||Statherian|Of the Strathearn Group (Willyama Supergroup). Overlies Ethiudna Subgroup.||||||24-FEB-10
35884|Saltbush Subgroup|23476|5|Briefly described|p50|||||||||
35884|Saltbush Subgroup|24289|5|Briefly described|p46|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group.||||||07-NOV-08
35884|Saltbush Subgroup|24431|5|Briefly described|p189 Fig. 1|||Of the Strathearn Group. Overlain by the Mount Howden Subgroup. Geological Province: Olary Domain.||||||
35884|Saltbush Subgroup|60485|5|Briefly described|p28 Fig. 2|||Of the Strathearn Group (Willyama Supergroup). Geological Province: Olary Domain. Equivalent to the Sundown Group (Broken Hill Domain).||||||24-FEB-10
35884|Saltbush Subgroup|61734|5|Briefly described|p52 Fig.2|Statherian|Statherian||1.69 Ga|Of the Strathearn Group||Overlies Bimba Formation (Curnamona Group). Is intruded by Lady Louise Suite. Is overlain by Mount Howden Subgroup.|Schistose, psammopelitic metasedimentary rocks with thin locally psammitic layers.|
35884|Saltbush Subgroup|61736|5|Briefly described|p665, p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Strathearn Group. Contains the Walparuta Formation. Age: </-1690Ma. Geological province: Olary Domain. Contains Mn-bearing ironstones.||||||24-FEB-10
35884|Saltbush Subgroup|62373|5|Briefly described|p503 Fig.2|||Of the Strathearn Group (Willyama Supergroup). Geological Province: Curnamona Province/Olary Domain.||||||24-FEB-10
35884|Saltbush Subgroup|62514|5|Briefly described|p748 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of Strathearn Group. Age: >1650Ma. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
35884|Saltbush Subgroup|62535|5|Briefly described|p665-666, p670-674|Paleoproterozoic|Paleoproterozoic|Hosts Mn-bearing ironstones, similar to those in the Broken Hill Group.|||Bimba, Plumbago, Walparuta Formations.||Mainly pelitic and psammopelitic schist with variable thin, planar psammite beds and occasional calc-silicate-rich ellipsoidal structures.|
35884|Saltbush Subgroup|62592|5|Briefly described|p16 Fig.2.2.|||Olary Domain, Curnamona Province. Equivalent to Sundown Group, and possibly a small part of the Broken Hill Group, in the Broken Hill Domain.||Unit in Strathearn Group.||||
35884|Saltbush Subgroup|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Olary Domain).||||||07-NOV-08
35884|Saltbush Subgroup|63102|5|Briefly described|p13-15,26-27,33-35,37,69|||Geological province: Olary Domain, Curnamona Province Of the Meningie Well, Weekeroo and Ameroo Hill areas. This unit is the stratigraphic equivalent of the combined Broken Hill and Sundown Groups of the Broken Hill Domain within the Olary Domain.||Unit of Strathearn Group.|Includes Walparuta Formation, Plumbago Formation and Oonarta Creek Formation|||22-OCT-19
35884|Saltbush Subgroup|63186|5|Briefly described|p67 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Strathearn Group (Willyama Supergroup). Geological Province: Olary Domain, Curnamona Province.||||||07-NOV-08
35884|Saltbush Subgroup|64742|5|Briefly described|p320, p321 Fig.3, p323, pp325-326. |||Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Strathearn Group.|Includes Bimba, Plumbago and Walparuta Formations.|||
35884|Saltbush Subgroup|64744|6|Mentioned|p353 Fig.4, p356. |Statherian|Statherian|Olary Domain.||Unit in Willyama Supergroup.||Is overlain by Mount Howden Subgroup.||
35884|Saltbush Subgroup|70657|5|Briefly described|p5, p33, p39|Statherian|Statherian|Conor (2000). In this study, it is raised to Group rank (see references to Saltbush Group p5, p6 Fig.1, p11-14, p33-34, p43).||Strathearn Group.||Overlies Plumbago Formation. Equivalent to the combined Broken Hill and Sundown Groups.||
35884|Saltbush Subgroup|72461|6|Mentioned|p6|||||||||
68094|Saltbush subgroup|60485|6|Mentioned|p30|||Informal - see Saltbush Subgroup.  Interlayered garnetiferous psammite, psammopelite and pelite.||||||
81156|Samphire granite|71413|4|Described|p31-40|Calymmian|Calymmian|Geological province: Gawler Craton. Subsurface only. Known from mineral exploration drilling and geophysics. Fractionated Hiltaba Suite intrusion, increasingly so from E-W in the northern part of the onshore portion, interpreted to have been sequentially emplaced. Appears as a north-south elongate irregular ellipsoidal body 55x23km wide in aeromagnetics. The Samphire granite has been dated at c. 1585 Ma (Jagodzinski and Reid 2017).|~1585 Ma|Unit of Hiltaba Suite.||Intrudes Warrow Quartzite, Broadview Schist,  Wandearah Formation and Hutchison Group. Unconformably overlain by Eocene (Kanaka beds) or Miocene sediments.|Includes: green granite, coarse- to medium-grained; mottled granite, green and white mottled, coarse to medium grained; red granite, red-coloured medium-grained.|19-JUN-19
39973|Sandison Subgroup, Upper|24195|6|Mentioned|p48|||Not intended as a formal name - see Sandison Subgroup||||||
40085|Sawpit Sandstone|24208|5|Briefly described|p169|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Penola Trough (Otway Basin).||||||
40085|Sawpit Sandstone|24209|6|Mentioned|p151|||Informally named by Lovibond et al (1995).||||||
40085|Sawpit Sandstone|24314|5|Briefly described|p61 Fig.2|Valanginian|Valanginian|See also Sawpit Shale.||||||30-NOV-04
40085|Sawpit Sandstone|24562|5|Briefly described|p8 Fig. 2|Hauterivian|Berriasian|Of the Crayfish Group.  Geological Province: Otway Basin.||||||
40085|Sawpit Sandstone|61547|6|Mentioned|p461 Fig.2. |Early Cretaceous|Early Cretaceous|||||Overlies Lower Sawpit Shale. Is overlain by Upper Sawpit Shale.||
40085|Sawpit Sandstone|63124|5|Briefly described|p48 Fig. 5.1|||Controversial nomenclature of Lovibond et al (1995) - in naming Sawpit Shale and Sawpit Sandstone as parts of Pretty Hill Formation. Geological Province: Otway Basin.||||||
40085|Sawpit Sandstone|63269|6|Mentioned|p606|||Details of oils and oil stains in named wells tabulated.||||||
40085|Sawpit Sandstone|63431|5|Briefly described|p677 Fig. 2|Valanginian|Valanginian|Occurs between the Upper and Lower Sawpit Shales. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
40085|Sawpit Sandstone|69297|5|Briefly described|p79|Hauterivian|Valanginian|Otway Basin. ||Crayfish Subgroup||Overlies the Casterton Formation. Overlain by the Pretty Hill Formation.|Siltstone.|
40085|Sawpit Sandstone|70077|6|Mentioned|Regional: Fig.4|Hauterivian|Valanginian|Otway Basin: Robe-Penola Trough. Is shown as Sawpit Shale/Sawpit Sandstone.||Crayfish Subgroup.||||
40085|Sawpit Sandstone|70379|5|Briefly described|p717, p719, p722-729, p731-732|Early Cretaceous|Early Cretaceous|Otway Basin. Widespread distribution across the Basin. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Mid-Valanginian.|c. 139-133 Ma.|Crayfish Group.||Overlies Sawpit Shale (equivalent). Is overlain by Pretty Hill Sandstone.|High-energy (dominantly coarse-grained) fluvial sediments.|
40085|Sawpit Sandstone|72050|5|Briefly described|p233 Fig.2, 235|||The middle of three units on the Kanawinka Terrace (Otway Basin) which together are equivalent to the Pretty Hill Formation.||Crayfish Group.||Equivalent to middle Pretty Hill Formation. Overlies Lower Sawpit Shale. Is overlain by Upper Sawpit Shale.||
40085|Sawpit Sandstone|73383|6|Mentioned|p15|||Otway Basin. Informal lithology-based unit.||Pretty Hill Formation||||
40085|Sawpit Sandstone|73594|5|Briefly described|p15-16, p45, p50-53|||Otway Basin. Southwards-thickening unit originally identified on seismic data, type section is in the Sawpit-1 well. Splits the Sawpit Shale into upper and lower 'members'. Maximum thickness in the hangingwall of the Kalangadoo Fault. Relatively high energy, braided fluvial system that passes upwards into meandering channels. Appears to be restricted to the Penola Trough.||Pretty Hill Formation||Overlies Lower Sawpit Shale, underlies Upper Sawpit Shale, underlies Eumeralla Formation on the Kawawinka Platform|Stacked, very-fine grained, upwards-fining quartzose sandstones.|
76881|Sawpit Sandstone Member|61547|6|Mentioned|p461. |Early Cretaceous|Early Cretaceous|||Unit in Pretty Hill Formation.||||
76881|Sawpit Sandstone Member|63267|5|Briefly described|p484, p485 Fig.2, p486, p496|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Sub-commercial discoveries of petroleum accumulations. Abbreviated to Sawpit Sandstone on p496.||Pretty Hill Formation.||Overlies lower Sawpit Shale member. Is overlain by upper Sawpit Shale member.||
73548|Sawpit Sandstone""|63124|6|Mentioned|p59|||Informal name of Lovibond et al (1995) - see also Sawpit Shale.||||||
40102|Sawpit Shale|24208|5|Briefly described|p169|Early Cretaceous|Early Cretaceous|Of the Crayfish Group.  Geological Province: Penola Trough (Otway Basin)||||||
40102|Sawpit Shale|24314|5|Briefly described|p61 Fig.2|Valanginian|Early Cretaceous|See also Sawpit Sandstone.||||||30-NOV-04
40102|Sawpit Shale|63124|5|Briefly described|p48 Fig. 5.1|||Controversial nomenclature of Lovibond et al (1995) - in naming Sawpit Shale and Sawpit Sandstone as parts of Pretty Hill Formation. Geological Province: Otway Basin.||||||
40102|Sawpit Shale|69297|5|Briefly described|p79|Hauterivian|Valanginian|Otway Basin. ||Crayfish Subgroup||Overlies the Casterton Formation. Overlain by the Pretty Hill Formation.|Siltstone.|
40102|Sawpit Shale|70077|6|Mentioned|Regional: Fig.4|Hauterivian|Valanginian|Otway Basin: Robe-Penola Trough. Is shown as Sawpit Shale/Sawpit Sandstone.||Crayfish Subgroup.||||
40102|Sawpit Shale|70379|5|Briefly described|p717, p719, p721, p724-732|Early Cretaceous|Early Cretaceous|Otway Basin. Distribution was restricted to rapidly subsiding, structurally controlled depocentres in the W of the Basin. Isopach map. Relationship of tectonic activity to sediment accumulation discussed in detail. Late Berriasian to early Valanginian.||Crayfish Group.||Overlies Casterton Formation. Is overlain by Sawpit Sandstone (equivalent).|Fluvio-lacustrine sediments.|
40102|Sawpit Shale|73594|4|Described|p45, p51, p55|||Otway Basin. Informal subdivision of the lower Pretty Hill Formation introduced by Lovibond et al. (1995). Split into upper and lower 'members' by the Sawpit Sandstone.||Pretty Hill Formation, lower part|Lower Sawpit Shale, Upper Sawpit Shale|Overlies McEachern Sandstone, underlies Pretty Hill Sandstone|Thick claystone unit.|
76883|Sawpit Shale Member, Lower|61547|6|Mentioned|p461. |Early Cretaceous|Early Cretaceous|||||Is overlain by Sawpit Sandstone.||
76882|Sawpit Shale Member, Upper|61547|6|Mentioned|p461. |Early Cretaceous|Early Cretaceous|||||Overlies the Sawpit Sandstone.||
42213|Sawpit Shale member, lower|24314|5|Briefly described|p61 Fig.2|Valanginian||Geological Province: Otway Basin. Informal - see Sawpit Shale.||||||
42213|Sawpit Shale member, lower|63267|5|Briefly described|p485 Fig.2, p486|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Abbreviated to Sawpit Shale(s) on p486.||Pretty Hill Formation.||Is overlain by Sawpit Sandstone Member.||
42214|Sawpit Shale member, upper|24314|5|Briefly described|p61 Fig.2|Valanginian|Valanginian|Geological Province: Otway Basin. Of the Otway Supergroup. Informal - see Sawpit Shale.||||||
42214|Sawpit Shale member, upper|63267|5|Briefly described|p485 Fig.2, p486|Early Cretaceous|Early Cretaceous|Penola Trough, Otway Basin. Abbreviated to Sawpit Shale(s) on p486. Cap seal for Sawpit Sandstone Member reservoir.||Pretty Hill Formation.||Overlies Sawpit Sandstone Member. Is overlain by Pretty Hill Formation.||
73549|Sawpit Shale""|63124|6|Mentioned|p59|||Informal name of Lovibond et al (1995) - see also Sawpit Sandstone.||||||
73757|Sawpit Shale, Lower|61547|6|Mentioned|p461 Fig.2. |Early Cretaceous|Early Cretaceous|||Unit in Pretty Hill Formation.||Is overlain by Sawpit Sandstone.||
73757|Sawpit Shale, Lower|63431|5|Briefly described|p677 Fig. 2|Berriasian|Berriasian|Informal name. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
73757|Sawpit Shale, Lower|72050|5|Briefly described|p233 Fig.2, 235, 239|||The lowest of three units on the Kanawinka Terrace (Otway Basin) which together are equivalent to the Pretty Hill Formation.||Crayfish Group.||Equivalent to lower Pretty Hill Formation. Is overlain by Sawpit Sandstone.||
73757|Sawpit Shale, Lower|73383|6|Mentioned|p15|||Otway Basin. Informal lithology-based unit.||Pretty Hill Formation||||
73757|Sawpit Shale, Lower|73594|5|Briefly described|p45 Fig.5.19, p51|||Otway Basin. Subdivision of the Sawpit Shale by Lovibond et al. (1995). Also written as lower Sawpit Shale p51.||Sawpit Shale||Overlies McEachern Sandstone, underlies Sawpit Sandstone|Includes thin, interbedded sandstone units.|
40086|Sawpit Shale, Upper|24208|5|Briefly described|p169|Early Cretaceous|Early Cretaceous|Informal name - see Sawpit Shale. Of the Crayfish Group.  Geological Province: Penola Trough (Otway Basin).||||||
40086|Sawpit Shale, Upper|61547|6|Mentioned|p461 Fig.2. |Early Cretaceous|Early Cretaceous|||Unit in Pretty Hill Formation.||Overlies Sawpit Sandstone.||
40086|Sawpit Shale, Upper|63431|5|Briefly described|p677 Fig. 2|Valanginian|Valanginian|Informal name. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
40086|Sawpit Shale, Upper|72050|5|Briefly described|p233 Fig.2, 235|||The highest of three units on the Kanawinka Terrace (Otway Basin) which together are equivalent to the Pretty Hill Formation.||Crayfish Group.||Equivalent to upper Pretty Hill Formation. Overlies Sawpit Sandstone.||
40086|Sawpit Shale, Upper|73383|6|Mentioned|p15|||Otway Basin. Informal lithology-based unit.||Pretty Hill Formation||||
40086|Sawpit Shale, Upper|73594|4|Described|p45 Fig.5.19, p51|||Otway Basin. Subdivision of the Sawpit Shale by Lovibond et al. (1995). Also written as upper Sawpit Shale p45.||Sawpit Shale|Jacaranda Ridge Sandstone|Overlies Sawpit Sandstone, underlies Pretty Hill Sandstone, unconformably underlies Eumeralla Formation|Interbedded succession of claystones and siltstones.|
42212|Sawpit sandstone member|24314|5|Briefly described|p61 Fig.2|Valanginian|Valanginian|Informal - see Sawpit Sandstone. Geological Province: Otway Basin.||||||
42212|Sawpit sandstone member|73356|6|Mentioned|p1|||[Cited as from Boult and Hibburt (2002), although probably written as Sawpit Sandstone member therein after capitalisation of Sandstone by Lovibond et al. (1995). Perhaps written without capitalization of sandstone herein to denote informal usage]. Obsolete / informal unit name; superseded by Sawpit Formation.||||||
29926|Schist Group|43052|6|Mentioned|p51|||Refers to Johns (1961)||||||
67976|Sellick Hill Formation, lower|44133|5|Briefly described|p8|||Informal name.||||||
72884|Sellick Hill Formation, middle|23981|6|Mentioned|p61|Early Cambrian|Early Cambrian|Informal - see Sellick Hill Formation.  Geological Province: Stansbury Basin.||||||
67977|Sellick Hill Formation, upper|44133|5|Briefly described|p10|||Overlain by Fork Tree Limestone (conformably).||||||
72883|Sellick Hill formation, lower|23981|6|Mentioned|p25|Early Cambrian|Early Cambrian|Informal - see Sellick Hill Formation.  Geological Province: Stansbury Basin.||||||
68692|Sellicks Hill Limestone|9124|6|Mentioned|Map Legend|Cambrian|Cambrian|||||||
28993|Semaphore Sands|23818|6|Mentioned|p217|||||||||
28993|Semaphore Sands|34180|6|Mentioned|p217|||||||||
28993|Semaphore Sands|68811|5|Briefly described|p85, p86, p128 tbl 15|Holocene|Holocene|Dunes are up to 12m high. ||Of Saint Kilda Formation.|||Aeolian dunes.|15-APR-20
26136|Serle Conglomerate Member|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Well-bedded pebbly sandstone.||||||
26136|Serle Conglomerate Member|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
26136|Serle Conglomerate Member|23411|6|Mentioned|Map Legend|||||||||
26136|Serle Conglomerate Member|29780|6|Mentioned|p34|||||||||
26136|Serle Conglomerate Member|30177|2|Defined|p129|Adelaidean|Adelaidean|See also p76.Member of Tapley Hill Formation. Type section:Approximately two miles north of TindeIpina Hut, lat. 30degrees04'56"S long. 139degrees 18'21"E to lat. 30degrees04'27"S long. 139degrees 19'02"E.||||||25-NOV-22
26136|Serle Conglomerate Member|30801|6|Mentioned|p5|||Tapley Hill Formation. Table P5-6.||||||
26136|Serle Conglomerate Member|30807|6|Mentioned|p103|||Suggested map symbol||||||
26136|Serle Conglomerate Member|67180|6|Mentioned|p602 Fig.2|Cryogenian|Cryogenian|Sturtian age, [formerly?] of Tapley Hill Formation, in Northern Flinders Ranges (Preiss et al. 1998).||||Underlies the Tindelpina Shale Member of Preiss at al (1998).||
26136|Serle Conglomerate Member|67979|4|Described|p529, p531, p535-p536, p541-2, p545|Sturtian||Post glacial stratigraphy unique to Tindelpina region. Lenticular nature of this unit means stratigraphic thickness varies from 0 to 305 m (Coats and Blissett 1971). Type section at Tindelpina Hut of Serle Conglomerate and Tindelpina Shale Member (Coats, in Thompson et al. 1964) displays different facies compared with other regions. Shortened name, Serle Conglomerate, used on p529 also.||Basal Tapley Hill Formation.||Unconformably (angular truncation/erosional) overlies Lyndhurst Formation, and transitionally (conformably) overlain by Tindelpina Shale Member.|Interbedded boulder conglomerates, sandstones, siltstones and shales.|22-SEP-14
81275|Shanahan Conglomerate|68205|6|Mentioned|p85|||Geological province: Curnamona Province. Contains strongly-foliated basement clasts related to an pre-Adelaidean unconformity tectonic event.||||||
67978|Shannon Formation, upper|44133|5|Briefly described|p33|||Geological Province: Amadeus Basin.||||||
82955|Sherbrook Group, Lower|72050|6|Mentioned|p233 Fig.2|||||||||
33955|Sherbrooke Group|22495|6|Mentioned|P221|||||||||
33955|Sherbrooke Group|22930|6|Mentioned|50|||||||||
33955|Sherbrooke Group|22932|6|Mentioned|22|||||||||
33955|Sherbrooke Group|24470|6|Mentioned|p473|||||||||
81745|Silsby Granite|67323|5|Briefly described|p37|||Southern Gawler Craton.|~1530 Ma (Hand et al., 2007).|||||
22848|Silverton Subgroup|24465|5|Briefly described|p353, 346|Early Cambrian|Early Cambrian|Introduced by Dyson et al. (1996) and included the Talkisker and Tapanappa Formations.||||||11-OCT-12
22848|Silverton Subgroup|60712|4|Described|p27,  p28 Fig. 1, p30 Fig. 3|Early Cambrian|Early Cambrian|Comprises Talisker Calc-siltstone, Karinya Shale and Tapanappa Fm - together, represent a major transgressive-regressive cycle. A preliminary sequence strat. of Kanmantoo Gp was erected due to study and interpretation of unconformities in this subgroup.||||||31-MAY-05
80384|Simmons Quartzite|71242|6|Mentioned|p10|||Member of the Tent Hill Formation of Thomson (1965).||||||07-FEB-18
80805|Sir Isaac Granite|68131|5|Briefly described|p3 Tb.1, p5, p65-70|||SW Eyre Peninsula. Appears as Sir Isaac Granites on p65 and p67.|2445 +/- 3 Ma.|||Equivalent to Kiana Granite.|A suite of syn-tectonic granites consisting of highly peraluminous bodies, granodiorites/diorites and Himalayan-style leucogranites. Cut by mafic dykes and high-strain to mylonitic zones.|
80805|Sir Isaac Granite|71859|5|Briefly described|p7, p9|Siderian|Siderian|Crops out on the northern coast of Coffin Bay Peninsula.|2445 +/- 4 Ma (Jagodzinski et al., 2006)|||Equivalent to the Dutton Suite.|Garnet- and cordierite-bearing K-feldspar-quartz-plagioclase-biotite granite.|06-MAR-19
29927|Sir Joseph Banks Group|43052|6|Mentioned|Fig. 4.17|||||||||
35694|Skates Hill Formation|23282|6|Mentioned|p53|||of the western Officer Basin - Savory Sub-basin. Stromatolites present. May correlate with Coominaree Dolomite||||||
35694|Skates Hill Formation|23557|5|Briefly described|p95 Fig.1|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||
35694|Skates Hill Formation|24183|5|Briefly described|p21|||Equivalent to the Backdoor Formation. Geological Province: Bangemall Basin.||||||
35694|Skates Hill Formation|50008|5|Briefly described|p46 Fig.3|Neoproterozoic||Of Sunbeam Group. Geological Province: Officer Basin.||||||
35694|Skates Hill Formation|64772|5|Briefly described|p15|Neoproterozoic|Neoproterozoic|Misspelt - correct place name in WA is Skates Hills. See Skates Hills Formation.||||||07-FEB-11
35694|Skates Hill Formation|65365|5|Briefly described|p10 Fig. 4|Cryogenian|Cryogenian|Northwestern Officer Basin. Includes stromatolite assemblage.||||||
35694|Skates Hill Formation|65366|5|Briefly described|p23, p23 Fig. 3, p24|Cryogenian|Cryogenian|Northwestern Officer Basin, Savory Sub-basin. Includes stromatolite assemblage.||||||19-MAR-12
35694|Skates Hill Formation|65454|5|Briefly described|p11|Cryogenian|Cryogenian|NW Officer Basin. Of Sunbeam Group. Contains Acaciella australica stromatolites suggesting temporal correlation with Bitter Springs Formation (Amadeus Basin) and Coominaree Dolomite (Adelaide Rift Complex); ie older than 800 Ma, and possibly older than 827 Ma. Inferred to be a lateral facies equivalent of Mundadjini Formation.||||||
29964|Skillogalee Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
29964|Skillogalee Formation|43057|6|Mentioned|Fig.2.26|||Probably misspelling of Skillogalee Dolomite||||||
29964|Skillogalee Formation|61732|6|Mentioned|p25|||Contains microfossils.||||||07-FEB-11
29964|Skillogalee Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Mundallio Subgroup.||||
78555|Skillolagee Dolomite|67502|6|Mentioned|p46, p57||Neoproterozoic|[Mis-spelling of Skillogalee]. Of the Adelaide Geosyncline. Suggested to have a time correlation with the Black River Dolomite and the lower Akademikerbreen Formation (Spitzbergen) (Calver, 1998).||Burra Group||||26-MAY-14
83515|Skylark Metamorphics|73155|5|Briefly described|p274, p277, p284-285|Statherian|Statherian|Mount Woods Domain, southern, western, northern. Forms an outer rim of the central Mount Woods Metamorphics in the domain, interpreted as part of hangingwall/upper plate of Mount Woods Metamorphic Core Complex. Variable magnetic response. May be broadly equivalent with Kennedy's Dam Metamorphics. See also Skylark Metasediments.|ca. 1750 Ma|||Intruded by Engenina Adamellite.|Orthogneiss and paragneiss.|
39208|Sleaford Complex granite gneiss|23731|6|Mentioned|p26|||Informal.||||||
68078|Sleaford complex|24526|5|Briefly described|p97 Fig. 3|||Informal - see Sleaford Complex.||||||
40179|Sleafordian Complex|24597|6|Mentioned|p529|||Informal reference to the Sleaford Complex.  Geological Province: Gawler Craton.||||||
67981|Smith Bay Shale, Upper|44133|6|Mentioned|p12|||Maximum Thickness: ~150m.||||||
67979|Smith Bay Shale, lower|44133|5|Briefly described|p6|||Of the Kanmantoo Group.||||||
67980|Smith Bay Shale, upper|44133|5|Briefly described|p6|||Of the Kangaroo Island Group.||||||
67982|Snowtown Sand|44133|5|Briefly described|p165 Fig. 10.11, 152 Fig. 10.2|Early Oligocene|Early Oligocene|Geological Province: Saint Vincent Basin.||||||
32472|Soft Marl Member|23818|5|Briefly described|p191|Late Eocene|Late Eocene|Of the Blanche Point Marls. Rich in siliceous sponge spicules.||||||
32472|Soft Marl Member|33330|14|Not recorded|p171|||||||||
32472|Soft Marl Member|34308|6|Mentioned|p191?|||Uppermost member of Blanche Point Marls.||||||
83483|Southern Yorke Peninsula mafic dykes|73493|5|Briefly described|p718-720, p722 Fig.9, p723 Fig.10|||Subdivision of Daly Head Metadolerite, geochemistry is comparable to Royston Head mafic dykes. See also p725 Fig.12. Also written as 'Southern Yorke Peninsula mafic dykes' p718. See also Southern Yorke Peninsula gabbro p720.||Daly Head Metadolerite|||Straight-sided mafic dykes. Gabbroic, mostly tholeiitic but some are transitional to calc-alkaline.|
30616|Spilsby Granite|65376|6|Mentioned|p98.|||Name replaced by Spilsby Suite.||||||
80055|Spilsby Suite granite|70405|6|Mentioned|p12 figure 4|Mesoproterozoic|Mesoproterozoic|Spencer Domain.|1500 Ma|||||21-SEP-17
68698|Spilsby Suite granitoids|60954|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton.||||||31-MAY-05
40402|St Peters Suite|22690|6|Mentioned|p312|||||||||
40402|St Peters Suite|24422|5|Briefly described|p87|Paleoproterozoic|Paleoproterozoic|Misspelt - see St Peter Suite. Age: ca. 1690-1620 Ma. Geological Province: Gawler Craton.||||||07-NOV-08
40402|St Peters Suite|60704|5|Briefly described|p686 Fig.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
40402|St Peters Suite|60707|5|Briefly described|p611|Paleoproterozoic|Paleoproterozoic|Probably misspelt - probably named for St Peter Island? Same as St Peter Suite, south of Ceduna, also mentioned?  Pale pink granite and monzogranites.  Age: 1627+/-4Ma (Flint et al 1990). Geological Province: Gawler Craton.  Saint is St in text..||||||07-NOV-08
40402|St Peters Suite|63020|5|Briefly described|p986, p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: 1620+/-4Ma. Geological Province: Gawler Craton (Nuyts Domain).||||||07-NOV-08
40402|St Peters Suite|64137|5|Briefly described|p1542 Fig.1  |Paleoproterozoic|Paleoproterozoic|||||||
40402|St Peters Suite|64726|6|Mentioned|p83 Fig.2, p84, p86.|Paleoproterozoic|Paleoproterozoic|Arc-type magmas with calc-alkaline affinities emplaced along the southwestern margin of the Gawler Craton. |c.1620-1605 Ma.|||||
40402|St Peters Suite|67621|6|Mentioned|p212|||Gawler Craton.|~1.62-1.61 Ga.||||Arc-type magmatism.|
40402|St Peters Suite|70831|5|Briefly described|p26||||c. 1647-1604 Ma|||||
40402|St Peters Suite|73298|5|Briefly described|p1071, p1072 Fig.1, p1073, p1085-1087|Statherian|Statherian|Gawler Craton, Nuyts Domain. Calc-alkaline affinities and juvenile eNd isotopic character suggest subduction-related genesis. 1608 +/- 8 Ma age from Reid et al. (2016). Locations in text include p1076, p1077 Tb.2, p1078 Fig.6, p1080 Fig.8, p1083 Fig.10.|1633-1608 Ma, 1608 +/- 8 Ma||||Bimodal. Includes felsic granitoids, equigranular granite with little to no foliation.|
40402|St Peters Suite|73429|6|Mentioned|p115|||Gawler Craton.||||||
78889|St. Peter Suite|62641|5|Briefly described|p277 Fig.1, p278. |Statherian|Statherian|Nuyts Domain. Subduction-related arc setting with accretion (to the Gawler Craton). Name misspelt in Fig. 1 as St. Peter's Suite.|1640-1620 Ma||||Mafic-felsic suite.|20-MAY-14
78889|St. Peter Suite|72934|6|Mentioned|p9, p12|Statherian|Statherian|[Misspelling of St Peter Suite]. Northern Gawler Craton. Similar in age and isotopic character to the rocks of the Coompana Province.|1630-1605 Ma|||||
78307|Stansbury Formation|65892|5|Briefly described|p9 Fig.4. |Early Cambrian|Early Cambrian|Yorke Peninsula.||||Overlies Corrodgery Formation. Is overlain by Moonan Formation.||
78307|Stansbury Formation|68735|6|Mentioned|p233 Fig.2, p235 Fig.3|Early Cambrian|Early Cambrian|Stansbury Basin.||||||10-APR-17
78307|Stansbury Formation|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Yorke Peninsula.||||||
72885|Stansbury limestone|23981|6|Mentioned|p23|Middle Cambrian|Middle Cambrian|Informal - see Stansbury Limestone. Geological Province: Stansbury Basin.||||||
69579|Stirling Sandstone (SA)|61237|6|Mentioned|p36|||May be a commercial name? Used as building stone, superseding the Tapley Hill and Glen Osmond Bluestones.||||||16-AUG-05
81712|Stony Dam Conglomerate''|71129|6|Mentioned|p98|Neoproterozoic|Neoproterozoic|Of Stuart Shelf. Contains intercalations of Beda Basalt, intepreted to be equivalent to Backy Point Formation.||||||21-OCT-19
25495|Stradbrooke Formation|22889|4|Described|p33 & p39|Adelaidean|Adelaidean|Stradbrooke Formation superseded by Stradbrooke Siltstone Member, as the unit has been downgraded from formation to member status, see p33 for details of change.||||||
25495|Stradbrooke Formation|30801|6|Mentioned|p5|||River Wakefield Group. Table P5-6||||||
25495|Stradbrooke Formation|32725|6|Mentioned|p6|||Geol. map||||||
25495|Stradbrooke Formation|34535|6|Mentioned|Fig.19|||||||||
25495|Stradbrooke Formation|34536|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
25495|Stradbrooke Formation|35328|6|Mentioned|Table 1|||||||||
25495|Stradbrooke Formation|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25495|Stradbrooke Formation|41404|4|Described|p92|||||||||
25495|Stradbrooke Formation|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
25495|Stradbrooke Formation|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Unit of River Wakefield group. Willouran.||||||
25495|Stradbrooke Formation|64796|6|Mentioned|p191 Fig.9|Neoproterozoic|Neoproterozoic|||Unit in River Wakefield Subgroup.||||
25495|Stradbrooke Formation|71237|14|Not recorded|p9, 18|||||||||
72296|Strathearn pelite|62514|6|Mentioned|p747 Fig. 2|||Refers to pelitic rocks within Strathearn Group. Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
25498|Stuart Pedoderm""|30804|6|Mentioned|p12|||Refers Jessup & Norris.||||||
25498|Stuart Pedoderm""|30919|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
79132|Stuart Range beds|69946|6|Mentioned|p3|||Ludbrook (1967). Subsequently Stuart Range Formation (Townsend and Ludbrook, 1975).||||||
79152|Stun Sail Boom River Granite|68314|5|Briefly described|p755 Fig.6, p759|Middle Cambrian|Middle Cambrian|Of Fanning, 1990. Delamerian Orogen. Age inferred from Fig.6. See also Stun Sail Boom Migmatite Complex.|503 +/- 4 Ma (Fanning, 1990).||||I-type.|
79153|Stun Sail Boom River Migmatite Complex|68314|6|Mentioned|p754, p756|Late Cambrian|Middle Cambrian|Of Fanning, 1990. Post-collision magmatic event. Shortened to Stun Sail Boom River Complex on p756. See also Stun Sail Boom River Granite.||||||
69394|Sturt Tillites|61153|5|Briefly described|p344-345 Fig. 1|||Unconformably overlain by Heavitree Quartzite and Bitter Springs Formation. Age: >750 Ma. Geological Province: Adelaide Geosyncline.||||||
29027|Sturtian Formation|39558|6|Mentioned|Table 2|||||||||
81696|Sturtian Group|63102|6|Mentioned|p46|||Of Adelaide Geosyncline.||||||
29928|Sturtian Series""|43052|6|Mentioned|p183|||||||||
29928|Sturtian Series""|43384|14|Not recorded|Map Legend||Proterozoic|||||||
80468|Sturtian Tillite""|71529|14|Not recorded|p1|||Replaced by Sturt Tillite.||||||
81710|Sugarloaf Dam Kimberlite''|71129|4|Described|p135, 136|Early Jurassic|Early Jurassic|Geological Province: Gawler Craton. Part of a Jurassic kimberlite province. Kimberlite intrusion is synchronous with tholeiitic basalts which extend parallel to the Pacific-facing subduction margin of Gondwana on Kangaroo Island, Tasmania, Antarctica and Africa. Intruded directly at the periphery of the interpreted melted mantle zone which produced these tholeiitic melts (Foden et al., 2008). Discovered by Stockdale Prospecting in 1973 by using stream sediment and surface loam sampling at increasing density (Stockdate Prospecting Ltd, 1974), indicated by kimberlitic garnet in sample concentrates. Occurs in the NE corner of SIX MILE HILL, covering an area 0.4km x 0.5km. Intersected in drillholes PSD-1 to PSD 30. Thickness: about 3m, up to 3.9m to the NW and thinning rapidly to the E and SE edge. Dating of rutile yielded age of c. 187 Ma, similar to that from the El Alamein Kimberlite, which may represent upper mantle thermal events just before emplacement of the kimberlite (Cooper and Morris, 2012).|187 Ma from rutile.|||Intrudes as a sill into Tregolana Shale Member.|Kimberlite sill; 50% olivine phenocrysts, 5-10% ilminite, 5-15% mica, rare garnets in a carbonate-serpentinite matrix.|21-OCT-19
81710|Sugarloaf Dam Kimberlite''|73234|6|Mentioned|p7|||[Written as 'Sugarloaf Dam Kimberlite']. Six Mile Hill. Occurs in the shallow subsurface as a thin sill within the Tregolana Shale Member. Related to similar kimberlite occurrences at El Alamein 10 km southwest of Port Augusta.||||Intrudes Tregolana Shale Member (Tent Hill Formation).||
35722|Suite 6|43052|6|Mentioned|p94, 97|Paleoproterozoic|Paleoproterozoic|Metavolcanic-granitic suite. Mount Painter Inlier.||||||07-NOV-08
23999|Summerfield Granodiorite|22766|5|Briefly described|Fig.2 p561|Ordovician|Late Cambrian|Age of unit 486+/-6 Ma. See also Fig.1 p560||||||
23999|Summerfield Granodiorite|42813|6|Mentioned|p24|||||||||
23999|Summerfield Granodiorite|42884|6|Mentioned|p10|||Superseded by Summerfield Intrusive Suite.||||||26-MAR-08
23999|Summerfield Granodiorite|44133|5|Briefly described|p55-56 Table 7.3|Ordovician|Ordovician|I-Type. Age: 486 +/- 6Ma.||||||
74088|Sutherland Formation|61732|5|Briefly described|p28 Fig. 13|Marinoan|Marinoan|Of the Upalinna Subgroup (Umberatana Group).  Includes the Cox Sandstone Member. Geological Province: Adelaide Rift Complex.||||||07-FEB-11
70563|Swanport Granite""|61525|6|Mentioned|p40|||Informal name - see Murray Bridge Granite.||||||02-JUN-06
26922|Talisker Calc-Siltstone|22581|5|Briefly described|p45|||Kanmantoo Group, Kanmantoo Basin. Overlies Backstairs Passage Formation. Overlain by Tappanappa Formation||||||
26922|Talisker Calc-Siltstone|22643|5|Briefly described|p191,fig3,6,7|Early Cambrian|Early Cambrian|||||||
26922|Talisker Calc-Siltstone|24465|5|Briefly described|p346 Fig.3|||Of the Inman Hill Subgroup, but superseded by Talisker Formation of the Bollaparudda Subgroup.||||||24-FEB-05
26922|Talisker Calc-Siltstone|40454|6|Mentioned|Fig.1|||||||||
26922|Talisker Calc-Siltstone|42225|6|Mentioned|Fig.4 P224|||||||||
26922|Talisker Calc-Siltstone|42243|5|Briefly described|p211|||||||||
26922|Talisker Calc-Siltstone|42499|5|Briefly described|Map legend|Cambrian||||||||
26922|Talisker Calc-Siltstone|42505|5|Briefly described|Map legend|Cambrian||||||||
26922|Talisker Calc-Siltstone|43703|6|Mentioned|Fig.1,p75|||||||||
26922|Talisker Calc-Siltstone|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Kanmantoo Group. Geological Province: Adelaide Fold Belt.||||||27-MAY-08
26922|Talisker Calc-Siltstone|73107|5|Briefly described|Map legend.|Early Cambrian|Early Cambrian|Kanmantoo Trough.||Kanmantoo Group.|||Laminated calcareous and non-calcareous siltstone and sulphidic siltstone. Interbeds of lenticular, laminated fine sandstone.|
69048|Talisker Calc-siltstone, upper|60712|6|Mentioned|p33|Early Cambrian|Early Cambrian|Informal - see Talisker Calc-siltstone.||||||
35820|Tanunda Creek granite|23317|6|Mentioned|378|||||||||
83695|Tanunda gneiss complex|73430|6|Mentioned|p497|||[Tanunda Granite p504 and Tanunda gabbro p505 are shown as localities.]|||||Includes tholeiitic mafic bodies.|
69049|Tapanappa Formation, lower|60712|6|Mentioned|p34|Early Cambrian|Early Cambrian|Informal - see Tapanappa Formation.||||||
34230|Tapely Hill Formation|22631|6|Mentioned|p178|||Age: Sturtian||||||
25515|Tapley Hill "slates"|36137|6|Mentioned|p14|||||||||
69578|Tapley Hill Bluestone|61237|5|Briefly described|p36|||Informal name. Commercial term for building stone quarried from the siltstone of Tapley Hill Formation in the Tapley Hill and Brighton area.||||||16-AUG-05
39679|Tapley Hill Formation equivalents|24175|6|Mentioned|p48|||Informal name.||||||
27906|Tapley Hill Slates|9124|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Blue-grey, laminated  alternating siltstones and slates, locally phyllitic.||||||
27906|Tapley Hill Slates|30048|4|Described|p129|||||||||
27906|Tapley Hill Slates|30982|6|Mentioned|p435|||||||||
27906|Tapley Hill Slates|31923|6|Mentioned|p9|||||||||
27906|Tapley Hill Slates|34959|6|Mentioned|p283|||||||||
27906|Tapley Hill Slates|41405|6|Mentioned|p161|||||||||
27906|Tapley Hill Slates|71237|14|Not recorded|p9|||||||||
26927|Tarcoola Beds|23818|6|Mentioned|p31|||Geological Province: Gawler Block. Recognised as an equivalent to the Corunna Conglomerate.||||||
26927|Tarcoola Beds|30518|6|Mentioned|p89|||||||||
26927|Tarcoola Beds|31034|6|Mentioned|p141|||||||||
26927|Tarcoola Beds|31542|6|Mentioned|p468|||||||||
26927|Tarcoola Beds|33468|6|Mentioned|Fig.2|||See also P203||||||
26927|Tarcoola Beds|33470|5|Briefly described|p463|||||||||
26927|Tarcoola Beds|34537|5|Briefly described|p31|||||||||
26927|Tarcoola Beds|34904|6|Mentioned|Fig. 1|||||||||
26927|Tarcoola Beds|35255|6|Mentioned|p7|||||||||
26927|Tarcoola Beds|36507|6|Mentioned|Fig.1|||||||||
26927|Tarcoola Beds|38068|4|Described|p67|||||||||
26927|Tarcoola Beds|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26927|Tarcoola Beds|39905|6|Mentioned|Fig.2|||||||||
26927|Tarcoola Beds|43094|5|Briefly described|p42|||||||||
73377|Tarcoola Formation Sediments|63276|6|Mentioned|p9 Fig. 13|||Informal reference to sediments of the Tarcoola Formation.||||||
73972|Tarcoola beds""|61556|5|Briefly described|p9-10 Figure|Carpentarian|Carpentarian|In Central Province - Wilgena Hill and Tarcoola Mines.||||||21-NOV-07
83951|Tarcoola-Kingoonya Volcanics|70738|6|Mentioned|p186|||Gawler Craton. Fig1 only. See also reference p187, to mafic GRV units including Tarcoola-Kingoonya (Konkaby Basalt).||||||
32548|Taringa alluvium|44199|14|Not recorded|p597|||late Tertiary - Quaternary.||||||
35696|Tarlina beds|23282|6|Mentioned|p56|||of Stainton et al (1988), superceded by Tarlina Sandstone.||||||
25519|Tartwaup Formation""|31848|6|Mentioned|p21|||Refers Ludbrook (1969,1971)||||||
25519|Tartwaup Formation""|32119|6|Mentioned|p483|||Refers Ludbrook (1969,1970)||||||
81711|Tassie Member''|71129|5|Briefly described|p108-110|Neoproterozoic|Neoproterozoic|Of Stuart Shelf. Upper of two informally named units used in the past by Australian Selection Pty Ltd, (1979). Carbonaceous and pyritic laminae shales reflect deposition below wave base during maximum flooding phase in a distal restricted marine environment with dysoxic conditions near the sea floor.||Old informal unit of Tapley Hill Formation.||Underlain by informal  'Lincoln Member'.|Monotonous succession of dark grey, carbonaceous and pyritic, laminated shales and siltstones.|22-NOV-19
81673|Tassie member''|70334|4|Described|p20,38,48-49|||Geological province: Gawler Craton. Of Stuart Shelf. Informal term used by exploration companies on the Stuart Shelf (Mason 1979). Thickness: up to 130m. Deepwater facies.||Unit of Tapley Hill Formation.||Underlain by Lincoln member.|Thick and monotonous sequence of dark grey graphitic shale; varying proportions of graphite, chlorite, quartz, feldspar and carbonate, occasional dolomite laminae.|
76915|Tatachilla Limestone|65375|6|Mentioned|p34 Fig.7.|Eocene|Eocene|Mis-spelling of Tortachilla Limestone. Shown as Upper Eocene||||||
42113|Teal Flat Volcanics""|60567|6|Mentioned|p37|||Informal - see Teal Flat Volcanics.||||||
42114|Teal Flat-Marne River Volcanics|60567|6|Mentioned|p39|||Informal name - collective term for Teal Flat Volcanics and Marne River Volcanics.||||||
42531|Telford Gravel, Lower|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|Geological Province: Murray Basin.||||||
42532|Telford Gravel, Upper|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|||||||
80387|Tent Hill Series|71242|6|Mentioned|p9|||Equivalent of the Lincoln Gap Flagstones.||||||
74123|Terrapina Granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Age: 1560Ma. Geological province: Gawler Craton.||||||07-FEB-11
37482|Terripinna Granite|24045|5|Briefly described|p554 Table 1|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
70624|Thackaringa Group, upper|62373|6|Mentioned|p508|||Informal reference to the upper part of the Thackaringa Group.||||||
25527|Thompson Creek formation|40439|6|Mentioned|p383|||||||||
75187|Thorndale Composite Migmatite|64741|5|Briefly described|p301 Fig. 4, p307|Paleoproterozoic|Paleoproterozoic|Overlies Clevedale Migmatite. Geological province: Broken Hill Domain. Comprises partially melted clastic metasediments.||||||07-FEB-11
76913|Throoka Formation|65375|6|Mentioned|p34 Fig.7.|Eocene|Eocene|[Formal name is Throoka Silts].||||||
28195|Throoka Silts|23768|5|Briefly described|p28 Fig.5|Eocene|Eocene|Geological Province: St Vincent Basin. Presented as Throoka Silt in figure.||||||30-MAR-05
28195|Throoka Silts|30251|6|Mentioned|p3|||Refs Stuart(1970)||||||
28195|Throoka Silts|33330|2|Defined|p157|Tertiary|Tertiary|See also p158. Overlies Muloowurtie Fm.||||||13-SEP-12
28195|Throoka Silts|35689|6|Mentioned|Fig.33|||Stratigraphic correlation, St.Vincent Basin.||||||
28195|Throoka Silts|38699|6|Mentioned|p12|||||||||
28195|Throoka Silts|41513|6|Mentioned|p45|||||||||
28195|Throoka Silts|41626|6|Mentioned|Fig.2|||||||||
28195|Throoka Silts|61155|5|Briefly described|p3, p17|Late Eocene|Late Eocene|Lagoonal deposits. Overlain by Rogue Formation; partly overlies Muloowurtie Formation. Age: 37.5-37Ma. Geological Province: St Vincent Basin.||||||
83522|Tidnamakurna Volcanics|73155|6|Mentioned|p281|Statherian|Statherian|Gawler Craton.|ca. 1790 Ma|||||
69913|Tidnamurka Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1800Ma. Geological Province: northern Gawler Craton. Mount is Mt in text of figure.||||||07-NOV-08
69913|Tidnamurka Volcanics|61936|6|Mentioned|p203|||In the Peake and Denison Inlier.||||||
69913|Tidnamurka Volcanics|64725|6|Mentioned|p58 Fig.2. |||Gawler Craton.||||||
69913|Tidnamurka Volcanics|64726|6|Mentioned|p83 Fig.2.|||||||||
69913|Tidnamurka Volcanics|66882|6|Mentioned|p114 Fig.11, p117, p120|Statherian|Statherian|NE Gawler Craton. Enriched in LREE. Possible source of c.1790 Ma zircons in Cleve Group.|1796 Ma|||||
69913|Tidnamurka Volcanics|71341|6|Mentioned|p196|||Peake and Denison inlier.|ca. 1790-1770 Ma||||Orthogneisses and volcanic rocks.|
24034|Tilterana Sandstone""|38926|5|Briefly described|p34|||||||||
24034|Tilterana Sandstone""|42238|6|Mentioned|p73|||||||||
67984|Timboon Sand""|44133|6|Mentioned|p147|||Superseded by Timboon Sandstone.||||||
79113|Tirari Member|69982|5|Briefly described|p31, p39|||Of Zang (1993), for the quartzose sandstone lithofacies of the Pando Formation. His nomenclature, however, has not been followed in full (see Mudrangie Sandstone for explanation). On p39, reasons are given for abandoning this name [apart from the prior claims of the Tirari Formation, also in SA, from at least 1967].||||||
33952|Tirrawarra Conglomerate""|22527|5|Briefly described|p1|||Replaced by Big Lake Suite in Moomba Field, Cooper Basin||||||09-MAY-13
33952|Tirrawarra Conglomerate""|69982|6|Mentioned|p63|||Brief thin section description.||||||
33950|Tirrawarra Sandstone""|22527|4|Described|p 1, 2, 3, Fig 6|||Replaced by Big Lake Suite, Moomba Field||||||
68759|Tirrawarra sands|61015|6|Mentioned|p44|||Informal - see Tirrawarra Sandstone.||||||
80505|Tjuninata Formation|63866|5|Briefly described|p203|||Mulga Park Domain, Musgrave Province.||Tjauwata Group||||
42425|Tollu Formation Volcanics|24496|5|Briefly described|p15|||See also Tollu Volcanics and Tollu Group. Geological Province: Musgrave Block.||||||
39856|Tollu Group volcanics|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Informal name.  Age: 1080-1050Ma.  Of the Bentley Supergroup.  Geological Province: Musgrave Block.||||||
39856|Tollu Group volcanics|44109|6|Mentioned|p166 Fig. 164|||Informal - see Tollu Group. ||||||
39856|Tollu Group volcanics|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Moderately to weakly magnetic. Of Bentley Supergroup. Geological Province: Musgrave Block.||||||22-FEB-05
68761|Toolachee Formation, lower|61015|6|Mentioned|p45|Triassic|Triassic|Informal name.  Contains gas.||||||
35227|Toolechee Formation|22969|5|Briefly described|p 55||Late Permian|||||||
39189|Toolina Limestone""|23768|5|Briefly described|p39, p111|||Informal - see Toolina Limestone.  Local facies of Wilson Bluff Limestone or possibly of Abrakurrie Limestone according to Li et al (1996).  Geological Province: Eucla Basin.||||||30-MAR-05
25696|Top Mount Sandstone Beds|22889|6|Mentioned|p31|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.||||||
25696|Top Mount Sandstone Beds|24175|3|Fully described|p11, 52|Neoproterozoic|Neoproterozoic|Of Emeroo Subgroup (Burra Group).  Conformably overlain by Willawilpa Formation.  Max. thickness: 1000m.||||||
25696|Top Mount Sandstone Beds|37854|2|Defined|p13|Adelaidean|Adelaidean|Earliest? Torrensian.||||||
25696|Top Mount Sandstone Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
25696|Top Mount Sandstone Beds|40294|6|Mentioned|Table 2|||||||||
25696|Top Mount Sandstone Beds|41403|6|Mentioned|p43|||||||||
25696|Top Mount Sandstone Beds|41404|3|Fully described|p88|||||||||
25696|Top Mount Sandstone Beds|42222|6|Mentioned|Table 1 P5|||||||||
25696|Top Mount Sandstone Beds|42238|5|Briefly described|Table 1 P75|||||||||
25696|Top Mount Sandstone Beds|43052|5|Briefly described|p177,Table 6.1|||Emeroo Subgroup||||||
25696|Top Mount Sandstone Beds|60718|5|Briefly described|p49 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3. Misspelling of beds.||Of Emeroo Subgroup (Burra Group).||||15-APR-11
25696|Top Mount Sandstone Beds|69019|4|Described|p38.|Neoproterozoic|Neoproterozoic|Proposed by Murrell (1977); defined by Forbes et al. (1981). Type section NE of Kingston Dam. Thickness varies from 106 to 1000 m. Displays a variety of shallow-water and evaporitic sedimentary structures.||Unit in Emeroo Subgroup.||Is overlain conformably by Willawalpa Formation.|Greyish medium- to coarse-grained quartzite, arkose and sandstone, medium to platy bedding; interbedded finely laminated dark grey siltstone; stromatolitic grey dolomite and limestone are interbedded with the upper parts.|
31854|Tor Granite|23451|6|Mentioned|p534|||||||||
31854|Tor Granite|23719|6|Mentioned|p21|||Also known as Wertigo Granite. Geological Province: Gawler Craton.||||||
31854|Tor Granite|40644|6|Mentioned|p133|||Of Miles (1954) - written as "Tor Granite".||||||
31854|Tor Granite|45003|6|Mentioned|p36|||||||||
77688|Torrens Formation (SA)|40442|6|Mentioned|Fig.23|||||||||
38731|Tortachilla Formation|24397|5|Briefly described|p234 Tb. 2|Eocene|Eocene|Geological Province: St. Vincent Basin.||||||
38731|Tortachilla Formation|70722|6|Mentioned|p217|Middle Eocene|Middle Eocene|Of St. Vincent Basin. Not current. See Tortachilla Limestone.||||||
29070|Tortachilla limestones|38290|6|Mentioned|p22|||||||||
69608|Tortichilla Limestone|61155|6|Mentioned|p3||Middle Eocene|Misspelt - see Tortachilla Limestone. Widespread fossiliferous bioclastic carbonates. ||||||
29946|Tournefort Dyke Swarm|22489|5|Briefly described|p12,p13|Statherian|Orosirian|||||||
29946|Tournefort Dyke Swarm|22494|6|Mentioned|p34|||||||||
29946|Tournefort Dyke Swarm|22629|6|Mentioned|p157|Proterozoic|Proterozoic|||||||
29946|Tournefort Dyke Swarm|43052|5|Briefly described|Table 4.4|||||||||
29946|Tournefort Dyke Swarm|65375|6|Mentioned|p13, p18.|Paleoproterozoic|Paleoproterozoic|Name (of Parker et al. 1987) replaced by Tournefort Metadolerite.||||||
80806|Tournefort Dykes|71859|6|Mentioned|p1|||Southern Gawler Craton. Formerly part of the Lincoln Complex.||||||07-MAR-19
69736|Tournefort Metadolerite dykes|24508|6|Mentioned|p30|||Informal - see Torunefort Metadolerite.  Geological Province: Gawler Craton.||||||19-SEP-05
78856|Tournefort mafic dyke suite|66882|6|Mentioned|p101|Statherian|Orosirian|Of Vassallo and Wilson, 2001.|c. 1800 Ma|||||
80483|Tournefort mafic dykes|63866|5|Briefly described|p5, p9, p20, p31|Statherian|Orosirian|Spencer Domain, Gawler Craton. The provided isotopic date is uncertain. Referred to as the Tournefort mafic dyke on p9.|c. 1812 Ma (Pb-Pb Kober age)|||Intrudes the Donington Suite.||
35690|Townsend beds|23288|6|Mentioned|Fig.18|||||||||
41712|Trangle Hill granite|50605|5|Briefly described|p(ii), 1.3, 9.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Olary 1590 Ma Supersuite. Age: ~1590Ma (Shrimp).||||||
80421|Tregalana Shales|71242|5|Briefly described|p9|||Of Miles (1954). See also Tregolana Shale p9, 10, 11.||Of Corunna Group.||||07-FEB-18
29076|Tregolana Shale Member""|41429|6|Mentioned|p223|||||||||
79407|Tregolana shales|70406|6|Mentioned|p117|||Obsolete name of Miles (1955).||||||
39971|Trezona Formation, Upper|24195|6|Mentioned|p48|||Not intended as a formal name - see Trezona Formation||||||
37134|Trezona formation|23562|6|Mentioned|p298|||Superseded by Trezona Formation.||||||
74486|Triangle Hill granite|24197|5|Briefly described|p32|Mesoproterozoic|Mesoproterozoic|In the Olary Domain. Part of the Regional Suite. Age: c. 1590Ma.||||||07-FEB-11
40349|Truro Lamprophyre|23932|5|Briefly described|p680 Fig. 8|Ordovician|Ordovician|See Truro Volcanics.  Age: ~470Ma.  Geological province: Adelaide Fold Belt.||||||
30498|Truro Volcanic suite|43190|6|Mentioned|p29|||Informal name. Normanville Group||||||
30498|Truro Volcanic suite|61307|6|Mentioned|p5|||Informal reference to the Truro Volcanics (Normanville Group).  Geological Province: Adelaide Fold Belt.||||||
42533|Tungkillo Limestone Member|23818|5|Briefly described|p101 Fig.43|Cambrian|Cambrian|Geological Province: Kanmantoo Trough. Of the Brukunga Formation.||||||24-JAN-05
28303|Tungkillo Marble Member|23818|6|Mentioned|p104|||Of the Brukunga Formation.||||||24-JAN-05
28303|Tungkillo Marble Member|30801|6|Mentioned|p5|||Brukunga Formation. Table P5-6||||||
28303|Tungkillo Marble Member|33471|6|Mentioned|p557|||||||||
28303|Tungkillo Marble Member|34536|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Lower to Middle Cambrian||||||
28303|Tungkillo Marble Member|34612|6|Mentioned|p104|||Dolomite||||||
28303|Tungkillo Marble Member|40856|5|Briefly described|p312|||||||||
28303|Tungkillo Marble Member|41947|6|Mentioned|p21|||||||||
28303|Tungkillo Marble Member|42499|5|Briefly described|Map legend|Cambrian||||||||
28303|Tungkillo Marble Member|44133|5|Briefly described|p15|||Of the Backstairs Passage Formation.||||||
28303|Tungkillo Marble Member|60712|5|Briefly described|p30 Fig. 3|Early Cambrian|Early Cambrian|Of the former Brukunga Formation (Kanmantoo Group).  Name now abandoned.||||||
28303|Tungkillo Marble Member|61307|5|Briefly described|p6 Fig. 3|Cambrian|Cambrian|Of the Backstairs Passage Formation (Kanmantoo Group). Geological Province: Adelaide Fold Belt.||||||
76771|Tunkilla Suite|64722|5|Briefly described|p14, 26|Statherian|Statherian|Mis-spelling of Tunkillia Suite; see Fig. 2 p3-6, p14.||||||11-APR-12
68707|Tunkilla Suite granites|60704|6|Mentioned|p697|Paleoproterozoic|Paleoproterozoic|Informal - see Tunkilla Suite. Age: 1690-1670 Ma (Ferris, 2001).||||||07-NOV-08
68085|Tunkillia Augen Gneiss|60484|6|Mentioned|p34 Fig. 2|||Name probably not formalised yet?  See also Tunkillia augen gneiss p32.  Geological Province: Gawler Craton.||||||06-MAR-13
68085|Tunkillia Augen Gneiss|69649|6|Mentioned|p53 Fig.21|||Appears in a generalised cross-section of the Tunkillia Prospect, from Standish et al. (1997).||||||
68087|Tunkillia Suite granite|24505|5|Briefly described|p9 Tb. 1||Paleoproterozoic|Informal - see Tunkillia Suite.  Intruded by Hiltaba Suite. Geological Province: Gawler Craton.||||||07-NOV-08
68087|Tunkillia Suite granite|60484|6|Mentioned|p35|||Informal - see Tunkillia Suite. See also Tunkillia Suite granitoids.||||||03-MAR-05
68087|Tunkillia Suite granite|60716|6|Mentioned|p6 (photo)|||Informal - see Tunkillia Suite.||||||
68088|Tunkillia Suite granitoids|24505|5|Briefly described|p9 Tb. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Tunkillia Suite.  Age: ~1680Ma.  Geological Province: Gawler Craton.||||||07-NOV-08
68088|Tunkillia Suite granitoids|60484|6|Mentioned|p32|||Informal - see Tunkillia Suite.  See also Tunkillia Suite granite.||||||
68088|Tunkillia Suite granitoids|60716|6|Mentioned|p7|||Informal name - see Tunkillia Suite||||||24-JAN-06
68086|Tunkillia augen gneiss|60484|5|Briefly described|p32|||Informal - see Tunkillia Augen Gneiss.  One of four untis of the Tunkillia Suite. Medium-grained to megacrystic augen gneiss containing coarse K-feldspar augen up to 8x15mm, and strongly deformed, finer subhedral plagioclase grains.||||||
28163|Turkey Hill beds|23282|6|Mentioned|p54|||of western Officer Basin. Synonymous with Chambers Bluff Tillite. of Townson (1985).||||||
28163|Turkey Hill beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|[Superseded by Turkey Hill Formation. CEBMar95]||||||11-MAY-06
28163|Turkey Hill beds|43756|6|Mentioned|p541|||||||||
29083|Turton Limestone|60958|6|Mentioned|Map Legend|||||||||
39219|Uley graphite|23731|6|Mentioned|p52|||Informal.  Commercial term?||||||
39219|Uley graphite|61725|6|Mentioned|p894|||Informal name. Equated with Cook Gap Schists.||||||
76826|Ulupa Formation|67030|6|Mentioned|p411 Fig. 5, p415|||Probable misnaming of Ulupa Siltstone.||||||26-APR-12
42440|Umbeara granites|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Biotite and biotite-muscovite granites, variably foliated, fine- to coarse-grained, dominantly xenolithic; intruded by veins and dykes of pegmatite, aplite, microgranite, granophyre. Geological Province: Musgrave Block.||||||12-JAN-05
42440|Umbeara granites|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Biotite granite, biotite-muscovite granite +/-garnet. Geological Province: Musgrave Block.||||||
42440|Umbeara granites|61154|6|Mentioned|p9,p26|Mesoproterozoic|Mesoproterozoic|Informal grouping of unnamed granites of the Umbeara region.  Age: 1591+/-9Ma (inherited xenocrystic zircons).||||||
39312|Umberataana Group|24400|5|Briefly described|p155 Tb.2, p156|Adelaidean|Adelaidean|Age:>600Ma. Ovelain by Wilpena Group, overlies Burra Group.||||||
72808|Umberatana Group, Lower|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Informal - see Umberatana Group. Also referred to as the Sturtian glacials, consisting mainly of glaciomarine diamictite, quartzite, laminated siltstone and partly turbiditic sequences.||||||07-FEB-07
72808|Umberatana Group, Lower|23351|6|Mentioned|283|||||||||
72808|Umberatana Group, Lower|24546|6|Mentioned|p2 - 4 Fig.3|||Equivalent to Yudnamutana Sungroup. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
72808|Umberatana Group, Lower|67870|5|Briefly described|p25|Neoproterozoic|Neoproterozoic||||||Sandstone, conglomerate, quartzite, shale, hematite.|
72809|Umberatana Group, Middle|23315|5|Briefly described|344|Neoproterozoic|Neoproterozoic|Informal - see Umberatana Group. Comprises thick succession of thinly laminated and partly calcareous siltstone of the tapley Hill Formation.||||||07-FEB-07
72810|Umberatana Group, Upper|23315|5|Briefly described|p346|Neoproterozoic|Neoproterozoic|Informal - see Umberatana Group. Dominated by  thinner successions of shale, sandy limestone||||||07-FEB-07
72810|Umberatana Group, Upper|24546|6|Mentioned|p2 - 4 Fig.3|||Geological Province: Adelaide Fold Belt.||||||16-JAN-08
72810|Umberatana Group, Upper|67870|5|Briefly described|p25|Neoproterozoic|Neoproterozoic||||||Sandstone, conglomerate, siltstone, dolostone, shale.|
29088|Umberumberka Formation|42090|5|Briefly described|p42|||Of Wasson (1979), now Qh2 middle Holocene strandline white sand deposits along the eastern shore and around islands of Lake Frome.||||||24-AUG-18
42426|Umutju Suite|24496|5|Briefly described|p14, 16|Mesoproterozoic|Mesoproterozoic|Age: ~1180-1140 Ma (Scimgeour et al., 1999). Felsic plutons - adamellite to diorite, commonly charnockite. Equivalent to Kulgera Suite. Geological Province: Musgrave Block.||||||
42426|Umutju Suite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Foliated to undeformed clinopyroxene- and/or hornblende-bearing porphyritic granite with rounded blue-grey phenocrysts of K-feldspar.  Geological Province: Musgrave Block.||||||
42426|Umutju Suite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Coarsely  porphyritic granite, porphyritic granite, granite. Geological Province: Musgrave Block.||||||14-JAN-05
42426|Umutju Suite|60683|5|Briefly described|p10 Tb. 1, p41|||Informal abbreviation of Umutju Granite Suite? See also p13.||||||
42426|Umutju Suite|61154|4|Described|p11-12|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite. Comprises Walytjatjata, Puka and Mantapayika Granites. Age: 1175+/-7 and 1120+/-9Ma.  Geological Province: Musgrave Block. See also p42 and p44 Appendix.||||||03-AUG-05
42426|Umutju Suite|63866|5|Briefly described|p207|Stenian|Stenian|Fregon Domain, Musgrave Province. Ages derived from Young et al, 2002 and are Pb-Pb Kober dates.|1175 +/- 7 Ma to 1120 +/- 9 Ma |Pitjantjatjara Supersuite||||
42426|Umutju Suite|67375|5|Briefly described|p178.|Mesoproterozoic|Mesoproterozoic|Of Edgoose et el., 2004.||Unit in Pitjantjatjara Supersuite.|Includes Umutju Granite.|||
42426|Umutju Suite|69436|5|Briefly described|p21:4, 8|Mesoproterozoic|Mesoproterozoic|Fregon Domain, Mann Ranges, Musgrave Province. May be related to the Mirtutu Suite in adjacent regions in WA.||Pitjantjatjara Supersuite.|Walytjatjata, Puka, Mantapayika Granites.||Variably affected by mylonitic deformation associated with the Petermann Orogeny.|12-JUL-16
35697|Ungoolya Formation""|23282|6|Mentioned|p59|||Of Dunster (1987), superseded by Ungoolya Group.||||||18-APR-06
38134|Ungoolya Group, Upper|23524|5|Briefly described|p222|Neoproterozoic|Neoproterozoic|Informal name - see Ungoolya Group.||||||
68319|Ungoolya Group, lower|24111|5|Briefly described|p215, p216|Neoproterozoic|Neoproterozoic|Informal name.  Geological Province: Officer Basin.  See also p215 Fig. 11.||||||
68319|Ungoolya Group, lower|61732|6|Mentioned|p89, p123|||Informal - see Ungoolya Group.||||||07-FEB-11
68320|Ungoolya Group, upper|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Informal name.  Geological Province: Officer Basin.  See also p215 Fig. 11.||||||
35723|Unit 3|43052|6|Mentioned|p151, Table 5.9, p150|Mesoproterozoic|Mesoproterozoic|Volcanics, schist, quartzite.||||||
41713|Uno shale""|50605|5|Briefly described|p8.6|||Of the Corunna Conglomerate. Geological Province: Gawler Craton & Curnamona Province.||||||
78873|Upalinna Subgroup, Lower|62903|6|Mentioned|p729|||Informal. Adelaide Rift Complex. Sag-phase sedimentation.||||Brighton Limestone and Upalinna Subgroup, Lower, overlie Tapley Hill Formation; is overlain by Upalinna Subgroup, Upper.||
78874|Upalinna Subgroup, Upper|62903|6|Mentioned|p729|||Informal. Adelaide Rift Complex. Marine transgression.||||overlies Upalinna Subgroup, Lower; is overlain by Yerelina Subgroup||
29885|Upper Albite Formation""|43052|5|Briefly described|p84|||||||||
25569|Upper Callanna Beds|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
25569|Upper Callanna Beds|24176|3|Fully described|p10|Adelaidean|Adelaidean|Informal name - see Callanna Beds.  Age is Willouran.  Geological Province: Mount Painter Province.||||||
25569|Upper Callanna Beds|30176|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
25569|Upper Callanna Beds|30801|6|Mentioned|p5|||Willouran. Table P5-6.||||||
25569|Upper Callanna Beds|32720|6|Mentioned|Table 1|||||||||
25569|Upper Callanna Beds|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
25569|Upper Callanna Beds|33468|6|Mentioned|p209|||||||||
25569|Upper Callanna Beds|34535|3|Fully described|p55|||Willouran. Fig.16||||||
25569|Upper Callanna Beds|34537|6|Mentioned|Fig.9|||||||||
25569|Upper Callanna Beds|34812|6|Mentioned|Table 9|||||||||
26968|Upper Gawler Range Volcanics|23481|5|Briefly described|p19 Fig 1|||Informal. Geological Province: Gawler Craton.||||||
26968|Upper Gawler Range Volcanics|23805|5|Briefly described|p4 Fig. 1|Mesoproterozoic|Mesoproterozoic|Informal.  Geological Province: Gawler Craton.||||||
26968|Upper Gawler Range Volcanics|24346|5|Briefly described|p98 Fig.1|Mesoproterozoic|Mesoproterozoic|Informal - see Gawler Range Volcanics.||||||
26968|Upper Gawler Range Volcanics|24597|5|Briefly described|p526 Fig. 1|Mesoproterozoic|Mesoproterozoic|Informal - see Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
26968|Upper Gawler Range Volcanics|39352|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26968|Upper Gawler Range Volcanics|43053|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Informal. Acid volcanics. Includes Yardea Dacite.||||||26-MAY-05
26968|Upper Gawler Range Volcanics|65376|6|Mentioned|p8 Fig.1.1. |Mesoproterozoic|Mesoproterozoic|Name replaced by Gawler Range Volcanics.||||||
26968|Upper Gawler Range Volcanics|65485|6|Mentioned|Fig 1|Mesoproterozoic|Mesoproterozoic|||||||
34111|Upper Mannum Formation|22626|6|Mentioned|446 fig 10|Early Miocene|Early Miocene|Geol province Murray Basin. Overlying unit Finnis Clay, underlying unit Lower Mannum Formation||||||
34109|Upper Morgan Cadell Marl|22626|6|Mentioned|446 fig 10|Middle Miocene|Middle Miocene|Geol province Murray Basin. Underlying unit Lower Morgan Limestone||||||
33876|Upper Willyama Supergroup|73516|6|Mentioned|p2, p3 Fig.1|||Curnamona Province.||||Unconformably underlies Benagerie Volcanic Suite||
72887|Uratanna formation|23981|6|Mentioned|p13|||Informal - see Uratanna Formation. Geological Province: Arrowie Basin.||||||04-FEB-08
29910|Victory Downs Dyke Suite""|43052|6|Mentioned|p165|||Synonym for Alcurra Dyke Swarm||||||
39240|Vivonne Bay granites|23996|6|Mentioned|p352|||Formal name not intended.  Geological Province: Adelaid Fold Belt.||||||07-MAR-05
39181|Vulcan Quartzite""|24475|6|Mentioned|p51|||Informal name of Western Mining Corp.||||||
81832|Wabuna Formation|68131|6|Mentioned|p42|Pleistocene|Pleistocene|Eyre Peninsula.||||||
75106|Waikerie Limestone|64769|6|Mentioned|p28|Pliocene|Pliocene|Name for dimension stone in South Australia.||||||21-APR-09
35706|Waitoona beds""|23282|6|Mentioned|p84|||Equivalent or younger than Stuart Range Formation. of Krieg (1973).||||||
25583|Wakefield Subgroup|22869|6|Mentioned|P37|||||||||
25583|Wakefield Subgroup|37461|6|Mentioned|Table 5.I|||||||||
25583|Wakefield Subgroup|38108|6|Mentioned|Table 1|||||||||
77475|Walkindi Formation|13516|6|Mentioned|p171 fig 12|Middle Triassic|Early Triassic|In Simpson Desert Basin.||||||
73835|Wallarah-Great Northern Coal|24471|4|Described|p32 Fig.4, p33|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Balgownie Coal Member. Geological Province: Sydney Basin.||||||07-FEB-11
29468|Wallaroo Formation|42966|6|Mentioned|p179|||Variation on reserved name Wallaroo Group?||||||
39160|Wallaroo Group""|24475|5|Briefly described|p46|Paleoproterozoic|Paleoproterozoic|Conor (1995). See Wallaroo Group.||||||07-NOV-08
34813|Wallatina Formation|22915|6|Mentioned|14|||Misspelling of Wallatinna Formation.||||||
75619|Wallatina Member|65313|5|Briefly described|p578 Fig. 6|Cambrian|Cambrian|Lowermost member of Observatory Hill Formation, Officer Basin. Underlies Parakeelya Alkali Member.||||||26-MAR-12
24070|Wallatinna Formation""|38022|6|Mentioned|p29|||||||||
79725|Walleroo Group|68021|6|Mentioned|p139|||Gawler Craton.||||||
79725|Walleroo Group|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic||c. 1760-1740 Ma|||||
82039|Walloway suite|67127|6|Mentioned|p172|Jurassic|Jurassic|A series of dykes and plugs of carbonatite. See also p87, p108, p106, p135.|||||Carbonatite.|10-NOV-20
34319|Wandearah Metasediments|22629|6|Mentioned|p152, fig2p147|Paleoproterozoic|Paleoproterozoic|Expected to be revised.||||||07-NOV-08
34319|Wandearah Metasediments|24475|5|Briefly described|p46|||Orginally named Wandearah Metasiltstone (Parker, 1993), now Wandearah Formation.||||||
34319|Wandearah Metasediments|50605|5|Briefly described|p8.6, 8.7|||Interlayered with Willamulka Volcanics. Geological Province: Gawler Craton & Curnamona Province.||||||
34319|Wandearah Metasediments|60954|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Gawler Craton.||||||07-NOV-08
34319|Wandearah Metasediments|65376|6|Mentioned|p101. |||Name replaced by Wandearah Formation. However, metasiltstone lithologies in the Bute area are now defined as the Wokurna Member.||||||
34319|Wandearah Metasediments|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic||c. 1760-1740 Ma|||||
34319|Wandearah Metasediments|72461|6|Mentioned|p6|||Gawler Craton.||||||
24073|Wandearah Metasiltstone|22629|6|Mentioned|p152|Statherian|Statherian|Expected to be revised in future.||||||
24073|Wandearah Metasiltstone|23719|5|Briefly described|p18|Paleoproterozoic|Paleoproterozoic|Age: 1763+/-14 Ma, 1750+/-7 Ma (U-Pb zircon). See also p17, table 4, p16 table 3. Of Wallaroo Group. Geological Province: Gawler Craton.||||||07-NOV-08
24073|Wandearah Metasiltstone|24475|5|Briefly described|p46|||Renamed Wandearah Metasediments, now superseded by Wandearah Formation.||||||
24073|Wandearah Metasiltstone|39344|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24073|Wandearah Metasiltstone|39349|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle ProterozoicE - M||||||07-NOV-08
24073|Wandearah Metasiltstone|39802|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24073|Wandearah Metasiltstone|40448|6|Mentioned|Table 1|||||||||
24073|Wandearah Metasiltstone|40644|6|Mentioned|p124 Fig. 3,  p136|Mesoproterozoic|Paleoproterozoic|Metamorphic age: 1561+/-30Ma (see Table 4, p135).||||||07-NOV-08
24073|Wandearah Metasiltstone|41256|4|Described|p5|||See also Fig.3||||||
24073|Wandearah Metasiltstone|41402|6|Mentioned|p35|||||||||
24073|Wandearah Metasiltstone|41667|6|Mentioned|Fig.3|||||||||
24073|Wandearah Metasiltstone|41972|6|Mentioned|p367|||||||||
24073|Wandearah Metasiltstone|42090|6|Mentioned|p19|||||||||
24073|Wandearah Metasiltstone|42167|6|Mentioned|Fig.4 P117|||||||||
24073|Wandearah Metasiltstone|42235|6|Mentioned|p132|||||||||
24073|Wandearah Metasiltstone|42357|6|Mentioned|p8|||||||||
24073|Wandearah Metasiltstone|42468|5|Briefly described|Fig. 1 P2|||||||||
24073|Wandearah Metasiltstone|43052|5|Briefly described|p67|||||||||
24073|Wandearah Metasiltstone|43141|6|Mentioned|p63,Fig.1|||||||||
24073|Wandearah Metasiltstone|65375|6|Mentioned|p21.|||Equivalent to Wokurna Member of the Wandearah Formation.||||||
24073|Wandearah Metasiltstone|65376|6|Mentioned|p101. |||Name replaced by Wandearah Formation. However, metasiltstone lithologies in the Bute area are now defined as the Wokurna Member.||||||
24073|Wandearah Metasiltstone|68158|5|Briefly described|p2, p4, p13, p15-16|||Mainly Yorke Peninsula; some outcrops on NE Eyre Peninsula. No age constraints. Sm-Nd values. Age and provenance discussed in detail.|1762 +/- 7 Ma (maximum depositional age).|Wallaroo Group.|||Khaki, thinly-bedded to laminated dolomitic metasiltstone and sandy micaceous metasiltstone. Minor pink, fine-grained, thinly-bedded sandstone interbeds. Red-brown medium- to coarse-grained, poorly sorted, thinly-bedded sandstone.|
24073|Wandearah Metasiltstone|71235|6|Mentioned|p8|||||||||
24073|Wandearah Metasiltstone|71341|6|Mentioned|p187 fig 6, p188 fig 7|||||||||
78616|Wanderah Metasediments|65390|5|Briefly described|p18, p23 Fig.3|Statherian|Statherian|Of Wallaroo Group, Moonta Domain, Gawler Craton. Also called Wanderah Meta-siltstone. Age of 1760 +/- 7 Ma from interbedded Moonta Volcanics. [Formal name is Wandearah Formation].||||||
39167|Wandilta Volcanics Member|24475|6|Mentioned|p51|||Probably misspelt - see Wandilta Amphibolite Member.||||||
76212|Wangary Paragneiss|67058|5|Briefly described|p476, p492.|Neoarchean|Neoarchean|Southern Gawler Craton.|c.2520 Ma (Swain et al. 2005).|Unit in Sleaford Complex.||||
76212|Wangary Paragneiss|68128|6|Mentioned|p7|||Gawler Craton.|ca 2510 Ma|||||
76886|Wangeripp Group|61547|6|Mentioned|p461. |Eocene|Paleocene|Mis-spelling of Wangerrip Group.||||||
40220|Wangerrip Group clastics|24202|5|Briefly described|p323 Fig. 12|||Informal - see Wangerrip Group.  Geological Province: Gambier Sub-basin.||||||
67967|Wangkonda Formation, upper|23981|6|Mentioned|p25|||Informal - see Wangkonda Formation.||||||
67967|Wangkonda Formation, upper|44133|5|Briefly described|p8|||Informal name.||||||
72888|Wangkonda limestone|23981|6|Mentioned|p13|||Informal - see Wangkonda Limestone. See also Wangkonda Formation (probably supersedes Wangkonda Limestone).||||||26-FEB-07
80722|Wankanki Suite|69640|6|Mentioned|p50||||ca. 1400 Ma|||||
24559|War Loan Beds|23054|5|Briefly described|p11|||||||||
24559|War Loan Beds|36733|2|Defined|p69|early Adelaidean|early Adelaidean|See also P33.||||||
24559|War Loan Beds|37854|6|Mentioned|Table 1|||||||||
24559|War Loan Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24559|War Loan Beds|40294|6|Mentioned|Table 2|||||||||
24559|War Loan Beds|41403|5|Briefly described|p67|||||||||
24559|War Loan Beds|43052|5|Briefly described|p175,Table 6.2|||of Curdimurka Subgroup.||||||
24559|War Loan Beds|44289|5|Briefly described|Map Legend||Neoproterozoic|||||||
24559|War Loan Beds|64796|6|Mentioned|p189 Fig.7, p200 Fig.10|Neoproterozoic|Neoproterozoic|||Unit in Callanna Group.||||
79141|Warburton Formation|65489|5|Briefly described|p1, p160|Paleozoic|Paleozoic|[Misspelling of Warburton Basin] Forms an extensive cover over several Proterozoic basins in Central Australia. Intraformational shale seal. Possible source of oil in Poolowanna Trough.||||||
79141|Warburton Formation|70823|6|Mentioned|p76|||||||Unconformably overlain by the Arrabury Formation.|Sedimentary and volcanic rocks.|
31753|Warcowie Dolomite|23211|6|Mentioned|p45|||Interpreted to be of deep water origin in Umberatana and Wilpena Groups.||||||
31753|Warcowie Dolomite|43845|5|Briefly described|Fig3 p43, 41,42||Neoproterozoic|In Umberatana Group||||||12-JUL-16
31753|Warcowie Dolomite|70407|5|Briefly described|p103 Fig 2, p112, 113|Neoproterozoic|Neoproterozoic|Age: Sturtian. Cap dolostone. Associated with sequence boundary.||Of Umberatana Group.||||
24561|Wardang Volcanics|22629|5|Briefly described|p152|Statherian|Statherian|Age: 1760Ma||||||
24561|Wardang Volcanics|23719|5|Briefly described|p17 table 4|Statherian|Statherian|Age: 1756+/-27 Ma. Geological Province: Gawler Craton.||||||
24561|Wardang Volcanics|24475|6|Mentioned|p54|||Superseded by Wardang Volcanics Member of  Weetulta Formation.||||||24-JUN-09
24561|Wardang Volcanics|39911|4|Described|p2|||||||||
24561|Wardang Volcanics|40644|6|Mentioned|p129|||Upper Yorke Peninsula.||||||13-AUG-08
24561|Wardang Volcanics|41402|6|Mentioned|p35|||||||||
24561|Wardang Volcanics|43052|5|Briefly described|p64|||Age of about 1734 Ma.||||||24-JUN-09
24561|Wardang Volcanics|50605|6|Mentioned|p8.7|Paleoproterozoic|Paleoproterozoic|Age: ~1734Ma.||||||07-NOV-08
24561|Wardang Volcanics|63866|5|Briefly described|p5, p9, p20, p31|Statherian|Statherian|Moonta Domain, Gawler Craton. Shortened to Wardang Volc on p9. |c. 1770 Ma (U-Pb zircon, Fanning et al., 2007)|||||
24561|Wardang Volcanics|65375|6|Mentioned|p47.|||Presumably author's shorthand for Wardang Volcanics Member.||||||
24561|Wardang Volcanics|65390|5|Briefly described|p18, p23 Fig.3|Statherian|Statherian|Of Wallaroo Group. Olympic Domain, Gawler Craton. Age of 1760 +/- 7 Ma from interbedded Moonta Volcanics.||||||
24561|Wardang Volcanics|69748|6|Mentioned|p182|Paleoproterozoic|Paleoproterozoic||||||Includes felsic rhyodacite.|
24561|Wardang Volcanics|72461|6|Mentioned|p6|||Gawler Craton.||||||
24561|Wardang Volcanics|73026|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|Northern Yorke Peninsula.|1772 +/- 14 Ma|Wallaroo Group||||
24561|Wardang Volcanics|73027|6|Mentioned|p7|Statherian|Statherian||1772 +/- 14 Ma (Fanning et al, 2007)|Wallaroo Group||||
24561|Wardang Volcanics|73030|6|Mentioned|p2149|Statherian|Statherian|Gawler Craton, Olympic Cu-Au Province.||||||
24561|Wardang Volcanics|73092|6|Mentioned|p3, p22|Statherian|Orosirian|Age is of magmatic crystallisation. Dated sample is rhyodacite from Port Victoria. [Authors ambiguously use this name as both synonymous with and separate to Wardang Volcanics Member. Note that ASUD lists that Wardang Volcanics was superseded by Wardang Volcanics Member].|1779 +/- 31 Ma, 1772 +/- 14 Ma|||||
24561|Wardang Volcanics|73493|5|Briefly described|p722|Statherian|Statherian|Yorke Peninsula.|1772+/-14 Ma|Wallaro Group||||
68079|Wardung Volcanics|24526|6|Mentioned|p99|Paleoproterozoic|Paleoproterozoic|Possibly misspelt?  (place name is Wardang in SA). Age: 1760Ma.||||||07-NOV-08
29437|Warina Sand""|42966|6|Mentioned|p91|||Same as Warina Sand.||||||
25600|Warragee Siltstone Member|42269|6|Mentioned|p335|||||||||
25600|Warragee Siltstone Member|44133|5|Briefly described|p27|||Of the Billy Creek Formation. Overlies: upper Ajax Limestone, upper Wilkawillina Limestone. Maximum Thickness: 370m.||||||
25600|Warragee Siltstone Member|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Billy Creek Formation. Red-green shale, dolomite and siltstone; tuff bands.||||||
69716|Warre Formation|23830|5|Briefly described|Fig. 6|Late Cretaceous|Late Cretaceous|Geological Province: Gambier Embayment, Otway Basin.||||||24-JAN-06
39670|Warrina Supergroup, upper|24175|6|Mentioned|p10|Neoproterozoic|Neoproterozoic|Informal name for Burra Group.  (Warrina Supergroup not covered in this study).||||||
42408|Wataru orthogneiss|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Birksgate Complex. Geological Province: Musgrave Block.||||||22-FEB-05
24082|Watchie Sandstone Member|36966|3|Fully described|p89|||||||||
24082|Watchie Sandstone Member|38022|6|Mentioned|Fig.8|||||||||
24082|Watchie Sandstone Member|38108|6|Mentioned|Table 1|||||||||
24082|Watchie Sandstone Member|42465|5|Briefly described|Map Legend|||||||||
24082|Watchie Sandstone Member|42469|4|Described|p41|||||||||
24082|Watchie Sandstone Member|42723|5|Briefly described|map legend|Miocene||||||||
24082|Watchie Sandstone Member|43048|4|Described|Table 3.|||||||||
24082|Watchie Sandstone Member|60955|5|Briefly described|Map Legend|Miocene|Eocene|Of the Mirikata Formation. Sandstones, siltstones and minor clays, partially silicified.||||||13-APR-05
24082|Watchie Sandstone Member|64696|5|Briefly described|p133 Figs.13,14 |Miocene|Miocene|||Of the Mirikata Formation.||||
82111|Wattleowie granite|72459|4|Described|p63-66, p73, p82-89, p94-99|Mesoproterozoic|Mesoproterozoic|Together with the Terrapinna Granite, White Well Granite, Golden Pole granite and the Petermorra Volcanics forms sub""group"" 2b of this report. Sheard (1997) notes this granite can be gradational into Terrapinna Granite. Often exhibits a complex, intermingled association in outcrop with the Terrapinna Granite. Displays decreasing LREE, Th, U and Nb with increasing silica. Potentially co-magmatic with the Terrapinna Granite.||Moolawatana Suite|||White to pale grey, medium to coarse-grained, equigranular biotite granite, which often has a mottled or spotted appearance.|
75083|Waukaloo Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Ethiudna Subgroup||||15-DEC-21
75083|Waukaloo Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75083|Waukaloo Formation|64944|5|Briefly described|p28 Fig. 1, p29 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain. Also defined as Weekaroo Formation by Laing (1996) - probably replaced by Waukaloo Formation? Fine-grained psammitic schist.||||||07-FEB-11
75083|Waukaloo Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Ethiudna Subgroup||Overlies the Peryhumuck Formation.||
75083|Waukaloo Formation|70657|4|Described|p14-15, p26, p29, p37, p41-42, p66|Statherian|Statherian|Curnamona Province; Olary Domain. Age inferred from Tb.1. No equivalent in Broken Hill Domain. Up to several hundred metres thick. Mn-enrichment mentioned.|~1715-1705 Ma|Uppermost Ethiudna Subgroup.||Overlies Peryhumuck and ?Whey Whey Formations. Underlies Portia Formation and Bimba Formation (Saltbush Group).|Fine-grained quartz-mica schist, locally manganiferous and baritic. Contains a prominent piemontite.|
75083|Waukaloo Formation|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Olary Domain, Curnamona Province.||Ethiudna Subgroup.||||
29128|Wearing Dolomite member""|42241|6|Mentioned|p181|||||||||
81891|Weednana Skarn|71322|5|Briefly described|p101|||Northern Eyre Peninsula. Hosts a magnetite deposit. Age is for Hiltaba Suite granite emplacement into Weedana deposit. See p135.|1584 +/- 5 Ma (SHRIMP U-Pb zircon).||||Leucogranite.|13-DEC-21
76772|Weekaroo Amphibolite|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Olary Block, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
29930|Weekeroo Amphibolite|23223|5|Briefly described|p46|||Of Broken Hill Group. Olary Domain.||||||23-JUN-08
29930|Weekeroo Amphibolite|43052|6|Mentioned|Fig. 4.21|||Of Willyama Supergroup.||||||
29930|Weekeroo Amphibolite|70657|6|Mentioned|p16, p30, p46|||See eg Forbes (1991). Described as an informal name; appears as Weekeroo amphibolite on p30 and p46. Subsequently the Montstephen Metabasalt.||||||
29844|Weekeroo Formation|22884|2|Defined|p40 Fig.1, p44||Paleoproterozoic|Of Broken Hill Group. Correlated with the Meningie Well Formation. Contains lenses of Bimba Sulphide Member, locally. Max.thickness: 500m. Massive amphibolite, quite heterogeneous, variably brecciated and altered to calc-silicate assemblages.||||||26-MAR-09
29844|Weekeroo Formation|63102|6|Mentioned|p34|||Geological province: Broken Hill Domain, Curnamona Province. Nomenclature of Laing (1996b). Now considered to be the upper gradational part of Tommie Watt Formation.||||||
29844|Weekeroo Formation|64944|5|Briefly described|p27, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Laing (1996).  The term Waukaloo Formation is used by Conor in this study - and has probably replaced Laing's Weekaroo prefix?||||||07-FEB-11
29844|Weekeroo Formation|70657|6|Mentioned|p30, p41|||Laing (1996). Previous suggestions of equivalence with Broken Hill Formation are incorrect (explained).||||||
29888|Weekeroo Schist""|43052|6|Mentioned|p87|||||||||
81697|Weekeroo amphibolite|63102|6|Mentioned|p14,30,39|||Geological province: Broken Hill Domain, Curnamona Province. Informal term by Forbes 1991, now refers to Montstephen Metabasalt.||||||
70625|Weekeroo group|62373|5|Briefly described|p515|||Informal group in the metabasite suite of the Curnamona Province - part of the Montstephen Metabasalt.||||||
78754|Weekerroo Amphibolite|61734|6|Mentioned|p55 Fig.3|Statherian|Statherian|[Mis-spelling of Weekeroo]||||||
79142|Weena Sandstone|65489|6|Mentioned|p39|||Warburton Basin. Potential reservoir sandstones.||||||
82035|Weetootla Formation|72489|6|Mentioned|p13 Fig.10, p11, p12 Fig9|Cryogenian|Cryogenian|Located in South Australia.||||||
82911|Weetula Formation|73165|5|Briefly described|p621|||Gawler Craton, Moonta Domain, northern Yorke Peninsula.||Wallaroo Group||Interlayered with Wandearah Formation. Intruded by the Matta Formation.|Bimodal A-type volcanics.|
35707|Welbourn Volcanics|23282|6|Mentioned|p95|||||||||
29445|Werrikooian Series|42966|6|Mentioned|p155|||Synonym of undifferentiated Loxton-Parilla Sands.||||||
39157|West Doora Schists and Gneisses|24475|6|Mentioned|p51|||Informal name of Lynch (1982), now superseded by Doora Member of Wandearah Formation.||||||
39156|West Doora Schists and Gneisses""|24475|6|Mentioned|p46|||Informal name of Lynch (1982).||||||
25617|Whenan member|41125|6|Mentioned|p32|||||||||
75084|Whey Whey Formation|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||
75084|Whey Whey Formation|62535|5|Briefly described|p666 Fig.3, p672|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Ethiudna Subgroup.||||
75084|Whey Whey Formation|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Olary Domain.||Ethiudna Subgroup||||15-DEC-21
75084|Whey Whey Formation|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75084|Whey Whey Formation|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Ethiudna Subgroup (Curnamona Group). Geological province: Olary Domain.||||||07-FEB-11
75084|Whey Whey Formation|66302|5|Briefly described|p36 Fig.9, p37, p39|Statherian|Statherian|Olary Domain, Curnamona Province. ||Ethiudna Subgroup||Overlies the Peryhumuck Formation.||
75084|Whey Whey Formation|70657|4|Described|p14-15|Statherian|Statherian|Curnamona Province; Olary Domain. Formerly the Whey-Whey Schist of Conor (2000). Age inferred from Tb.1. No equivalent in Broken Hill Domain.|~1715-1705 Ma|Ethiudna Subgroup||Overlies Peryhumuck Formation. Underlies Waukaloo Formation. No equivalent in Broken Hill Domain.|Upward-fining metasediments from psammitic and psammopelitic to more pelitic.|
80368|Whey-Whey Schist|63102|6|Mentioned|p20,22|||Geological province: Olary Domain, Curnamona Province.  Superseded; see Whey-Whey Formation.||||||
80368|Whey-Whey Schist|70657|6|Mentioned|p28|||Conor (2000). Subsequently the Whey-Whey Formation.||||||
77520|White Hill Gabbro|64135|6|Mentioned|p1501.|Mesoproterozoic|Mesoproterozoic|Mount Woods Inlier.||||||16-JAN-15
83513|White Hills Complex|73155|6|Mentioned|p265, p278|Calymmian|Calymmian|Mount Woods Domain, southern. See also White Hill Complex.|ca. 1562 Ma|||||
67968|White Point Conglomerate, upper|44133|5|Briefly described|p27|||Geological Province: Stansbury Basin.||||||
83358|Whyalla Formation|73227|6|Mentioned|p28|||[Probably a variation on Whyalla Sandstone].||||||
37137|Whyalla formation|23562|6|Mentioned|p304|||||||||
34553|Wilara Dolomite|22746|6|Mentioned|p528|||||||||
69216|Wilari Dolomite|60565|6|Mentioned|p18|Neoproterozoic|Neoproterozoic|Carbonates||||||
23198|Wilcolo Sandstone|22927|6|Mentioned|43|||Geol province Adelaide Geosyncline||||||
23198|Wilcolo Sandstone|23180|6|Mentioned|p35|||of the Bunyeroo Formation [?? Is it a member? see p38]||||||
23198|Wilcolo Sandstone|23211|6|Mentioned|p41,43,44,46 Fig.2|||Cobble Conglomerate. of Aruhna Subgroup.||||||
23198|Wilcolo Sandstone|24195|5|Briefly described|p44, p45 Fig.3|||Parent: Aruhna Subgroup. Underlying Unit: ABC Range Quartzite||||||
23198|Wilcolo Sandstone|24586|5|Briefly described|p51 Fig. 2|Adelaidean|Adelaidean|Of the Aruhna Subgroup (Wilpena Group, Heysen Supergroup). Geological Province: Adelaide Geosyncline.||||||13-MAY-16
23198|Wilcolo Sandstone|43845|5|Briefly described|Fig3 p43, 42,46||Neoproterozoic|In Wilpena Group||||||12-JUL-16
23198|Wilcolo Sandstone|70406|5|Briefly described|p125|||||Of Aruhna Subgroup.||Overlies ABC Range Quartzite. May be equivalent to the top of the Simmens Quartzite.||
23198|Wilcolo Sandstone|70407|4|Described|p107-108, 102, 103, 105, 106,112|Neoproterozoic|Neoproterozoic|Age: Ediacaran. Type Section designated in Wilcolo Creek, 2 km south of Bunyeroo Gorge (lat. 31deg25'10" S, 138deg33'12" E. ?3-?50m thick. Fluvial at base to shoreface tidal at top.||Of Aruhna Subgroup. Incised valley into ABC Range Quartzite. ||Disconformably overlies ABC Range Quartzite. Conformably overlain by Bunyeroo Formation. Unconformably overlain by Wonoka Formation.|Channel-fill facies to estuarine to shallow marine shoreface tidal. Sandstone, quartzite, pebble to cobble conglomerate, shale.|13-MAY-16
75840|Wilgena Hill Jaspelite|65385|6|Mentioned|pS128 Fig. 2|||Typo for Wilgena Hill Jaspilite. Gawler Craton. Jaspilite and banded iron formation.||||||08-MAR-12
81861|Wilgena Hill Jaspellite|68128|5|Briefly described|p53|Palaeoproterozoic|Palaeoproterozoic|Gawler Craton.|||||Jaspilite and banded iron formation.|
82112|Wilgena Jaspilite|72459|6|Mentioned|p51|Palaeoproterozoic|Palaeoproterozoic|Wilgena, deposited in shallow localised basins.|ca. 1730-1700 Ma|||||
78306|Wilkawilina Limestone|68735|5|Briefly described|p233 Fig.2|||Misspelt Wilkawillina Limestone: see references p233-234.||||||10-APR-17
37187|Wilkawillina Formation|23562|5|Briefly described|p295 fig.2|Cambrian|Cambrian|||||||
40389|Wilkawillina Formation, Lower|24484|6|Mentioned|p815|||Informal name||||||
40390|Wilkawillina Formation, Upper|24484|6|Mentioned|p815|||Informal name||||||
29144|Wilkawillina Limestone, Upper|24484|5|Briefly described|p803 Fig.3|Cambrian|Cambrian|Unconformably overlain by the Lower Wilkawillina Limestone. Unconformably overlain by the Billy Creek Formation.||||||
29144|Wilkawillina Limestone, Upper|42011|4|Described|p459|||See also.Fig.3 P458||||||
29144|Wilkawillina Limestone, Upper|42213|6|Mentioned|Fig.2 P473|||||||||
29144|Wilkawillina Limestone, Upper|42226|6|Mentioned|Fig.4 P234|||||||||
29144|Wilkawillina Limestone, Upper|42458|5|Briefly described|Fig.2 P699|||||||||
29144|Wilkawillina Limestone, Upper|64319|5|Briefly described|p354, p356 Fig.2  |Early Cambrian|Early Cambrian|Separated from the Lower part by the Flinders Unconformity: a distinctive red stromatolitic horizon, and paleokarst surfaces.||Unit in Ajax Limestone.|||Abundant archaeocyathid fossils, and grades from a white to light-grey lime mud to a buff-coloured algal laminated and stromatolitic dolomite.|
29144|Wilkawillina Limestone, Upper|68735|6|Mentioned|p235 Fig.3|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
29144|Wilkawillina Limestone, Upper|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||Of the Hawker Group.||||
29144|Wilkawillina Limestone, Upper|70835|6|Mentioned|p336|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||||Overlies Bunkers Sandstone. Is overlain by Edeowie Limestone.||
67969|Wilkawillina Limestone, lower|44133|5|Briefly described|p4 Fig. 7.2, 23|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Disconformably overlies: Brachina Formation||||||
67969|Wilkawillina Limestone, lower|60889|4|Described|p245 Fig.2, p247-50, p252-3|Early Cambrian|Early Cambrian|Thickness: 340 m. Shelf limestone succession. Arrowie Basin. Also shown as Lower Wilkawillina Limestone.|>528 Ma.|Hawker Group||Disconformably overlies Woodendinna Dolomite. Transitions into Wirrapowie Limestone. Is overlain by Mernmerna Formation.|Limestone.|22-SEP-17
79374|Wilkawillina Limestone, middle|60889|4|Described|p245 Fig.2, p247 Fig.4, p248, p249 Fig.6|Early Cambrian|Early Cambrian|Platformal carbonates. Thickness varies greatly: 100-500m up to more than 2500m in Nepabunna Trough. Arrowie Basin.|525 +/- 8.0 Ma.|Hawker Group||Overlies Mernmerna Formation. Is overlain (disconformably?) by Bunkers Sandstone.|Carbonates.|22-SEP-17
81436|Wilkawillina Limestone, middle""|70833|6|Mentioned|p186|Cambrian|Cambrian|Of Arrowie Basin. Nomenclature of Gravestock and Hibburt 1991. Replaced by Second Plain Creek Member.||||||21-AUG-19
67970|Wilkawillina Limestone, upper|44133|5|Briefly described|p4 Fig. 7.2, 23, 24, 26|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Overlies; Wilkawillina Limestone, lower.||||||
67970|Wilkawillina Limestone, upper|60889|5|Briefly described|p249|Early Cambrian|Early Cambrian|Highstand tract. Three archaeocyathid-rich biohermal complexes described.|~524-523 Ma.|Hawker Group||Disconformable(?) beneath Coads Hill Member (Billy Creek Formation). Overlies Oraparinna Shale.||22-SEP-17
82034|Wilkiwillina Limestone|72489|6|Mentioned|p12 Fig.9, p13 Fig.10|Cambrian|Cambrian|||||||
24107|Willalinchina Formation|42375|6|Mentioned|p79|||Variation of Willalinchina Sandstone. Formerly part of Watchie Sandstone.||||||
39182|Willamulka Metabasalt Member|24475|6|Mentioned|p49 Tb.1|||Misspelt - see Willamulka Volcanics Member.||||||
39182|Willamulka Metabasalt Member|65375|6|Mentioned|p21.|||Name replaced by Willamulka Volcanics Member.||||Intercalated with Wokurna Member.||
25628|Willouran Formation|36083|6|Mentioned|p469|||||||||
29147|Willouran Series""|37854|6|Mentioned|p7|||||||||
29147|Willouran Series""|40294|6|Mentioned|Table 1|||||||||
29147|Willouran Series""|42238|4|Described|p73|||||||||
25629|Willunga Slate|23731|5|Briefly described|p27|||Of Tapley Hill Formation.||||||
25629|Willunga Slate|24288|5|Briefly described|p32|Neoproterozoic|Neoproterozoic|Of Tapley Hill Formation.||||||
25629|Willunga Slate|32510|6|Mentioned|p104|||||||||
25629|Willunga Slate|40499|6|Mentioned|p151|||||||||
25629|Willunga Slate|64769|6|Mentioned|p27|||SA. Dimension stone name. From the Tapley Hill Formation.||||||06-MAY-09
68096|Willyama Supergroup, Lower|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Geol province Broken Hill - Olary Domain||||||
68096|Willyama Supergroup, Lower|60485|6|Mentioned|p29 Fig. 3|||Informal - see Willyama Supergroup.  In this context is referring to the Curnamona Group.||||||28-APR-05
68096|Willyama Supergroup, Lower|62373|5|Briefly described|p504 Fig.3|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup.||||||07-NOV-08
68096|Willyama Supergroup, Lower|63102|6|Mentioned|p6,9,11,22|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona Province.Also known as Curnamona Group.||||||
68096|Willyama Supergroup, Lower|63489|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup. Represented here as undifferentiated rocks and associated granitoids.||||||07-NOV-08
68096|Willyama Supergroup, Lower|64726|6|Mentioned|p83 Fig.2.|||||||||
68096|Willyama Supergroup, Lower|65220|6|Mentioned|p21 Fig.3|Statherian|Statherian|1715-1690 Ma||||||10-DEC-09
68096|Willyama Supergroup, Lower|68315|6|Mentioned|p764|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent LP-HT amphibolite- to granulite-grade metamorphism in the c.1610-1590 Ma Olarian Orogeny.||||||
68096|Willyama Supergroup, Lower|70657|5|Briefly described|p6 Fig.1|Statherian|Statherian|Curnamona Province.||Willyama Supergroup.|Thackeringa, Rantyga and Curnamona Groups.|||
68096|Willyama Supergroup, Lower|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Curnamona Province.|1720-1700 Ma.|||||
68096|Willyama Supergroup, Lower|73021|6|Mentioned|p224|||||||||
68096|Willyama Supergroup, Lower|73524|6|Mentioned|p3 Fig.1|||||||||
68098|Willyama Supergroup, Sub-|60485|6|Mentioned|p29 Fig. 3|||Informal reference to the substratum beneath the Willyama Supergroup rocks.  Not intended as a formal name.||||||03-MAR-05
68097|Willyama Supergroup, Upper|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Informal subdivision of Willyama Supergroup Geol province  Broken Hill-Olary Domain Age Range C1700 Ma to C1650 Ma||||||
68097|Willyama Supergroup, Upper|60485|5|Briefly described|p27 Fig. 1|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup.||||||07-NOV-08
68097|Willyama Supergroup, Upper|62373|5|Briefly described|p504 Fig.3|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup.||||||07-NOV-08
68097|Willyama Supergroup, Upper|63102|6|Mentioned|p6,11,22|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona Province. Also known as Strathearn Group in Olary Domain.||||||
68097|Willyama Supergroup, Upper|63489|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup. Represented here as undifferentiated rocks.||||||07-NOV-08
68097|Willyama Supergroup, Upper|64726|6|Mentioned|p83 Fig.2.|||||||||
68097|Willyama Supergroup, Upper|65220|6|Mentioned|p21 Fig.3|Statherian|Statherian|1650-1600 Ma||||||10-DEC-09
68097|Willyama Supergroup, Upper|68315|6|Mentioned|p764|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent LP-HT amphibolite- to granulite-grade metamorphism in the c.1610-1590 Ma Olarian Orogeny.||||||
68097|Willyama Supergroup, Upper|70657|5|Briefly described|p6 Fig.1||Statherian|Curnamona Province.||Willyama Supergroup.|Sundown, Paragon, Strathearn, and upper Saltbush Groups.|||
68097|Willyama Supergroup, Upper|70858|6|Mentioned|p31, 33|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Close in age to Wernecke Supergroup, Yukon; suggested source of detrital zircons in the latter.|1690-1640 Ma.|||Equivalent to upper Strathearn Group (Olary Domain); and Sundown and Paragon Groups (Broken Hill Domain).||
68097|Willyama Supergroup, Upper|73021|6|Mentioned|p224|||||||||
68097|Willyama Supergroup, Upper|73524|6|Mentioned|p3 Fig.1|||||||||
70626|Willyama Supergroup, lower|62373|5|Briefly described|p503|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup. Age: ca 1715-1700 Ma.||||||07-NOV-08
70626|Willyama Supergroup, lower|63186|5|Briefly described|p68|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup - referred to in this study as the lower plate. Comprises Thackaringa and Curnamona Groups in Broken Hill and Olary Domains respectively. These lower rocks have been intruded by the felsic Rasp Ridge and Hores Gneisses.||||||03-NOV-22
70626|Willyama Supergroup, lower|63866|6|Mentioned|p38|||Dominantly shallow water successions.||||||
70626|Willyama Supergroup, lower|73429|5|Briefly described|p107-108|||Curnamona Province. Oxidised chemical composition, separated from upper Willyama Supergroup by regionally extensive redox boundary. Shown as Lower Willyama Supergroup p106 Fig.2.|||Curnamona Group, Thackaringa Group|||
70626|Willyama Supergroup, lower|73524|5|Briefly described|p3-4|||Rift-phase metasediments.||Willyama Supergroup|Thackaringa Group, Broken Hill Group, Sundown Group|Intruded by Silver City Suite||
68033|Willyama Supergroup, upper|50081|6|Mentioned|p43|||Informal - see Willyama Supergroup||||||
68033|Willyama Supergroup, upper|63186|5|Briefly described|p69|Paleoproterozoic|Paleoproterozoic|Informal - see Willyama Supergroup - referred to in this study as the upper plate. Comprises Sundown and Paragon Groups in Broken Hill Domain, and Strathearn Group in Olary Domain. Intruded by the felsic Rasp Ridge and Hores Gneisses.||||||07-NOV-08
68033|Willyama Supergroup, upper|63866|6|Mentioned|p38|||Dominantly shallow water successions.||||||
68033|Willyama Supergroup, upper|73429|5|Briefly described|p107-108|||Curnamona Province. Reduced chemical composition, separated from lower Willyama Supergroup by regionally extensive redox boundary. Shown as Upper Willyama Supergroup p106 Fig.2.|||Saltbush Group, Broken Hill Group, Sundown Group, Paragon Group, Strathearn Group|||
36755|Willyama Supersuite|23775|6|Mentioned|p721|||See Willyama Supergroup.||||||22-SEP-09
38976|Wilochra Subgroup|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
38976|Wilochra Subgroup|67030|5|Briefly described|p409 Fig. 2|Cryogenian|Cryogenian|[Mis-spelling of Willochra Subgroup].|||Elatina, Wilmington and Angepena Formations.|Underlies the Nuccaleena Formation and Seacliff Sandstone, overlies the Brighton Limestone and Tapley Hill Formation.||26-APR-12
29150|Wilpena Group Siltstones|31729|6|Mentioned|p111|||Geological map||||||
42534|Wilpena Group, Lower|23818|5|Briefly described|p73 Fig.27|Adelaidean|Adelaidean|Extends from Nuccaleena Formation (bottom) to the base of the Bunyeroo Formation (top).||||||24-JAN-05
42535|Wilpena Group, Upper|23818|5|Briefly described|p73 Fig.27|Adelaidean|Adelaidean|Extends from base of the Bunyeroo Formation (bottom) to the Pound Quartzite.||||||
67971|Wilpena Group, lower|44133|5|Briefly described|p7|||Discordiantly overlain by the Mount Terrible and Winulta Formations.||||||
67972|Wilpena Group, upper|24586|6|Mentioned|p51|Adelaidean|Adelaidean|Informal - see Wilpena Group.  Includes the Wonoka Formation. Geological Province: Adelaide Geosyncline.||||||
67972|Wilpena Group, upper|44133|6|Mentioned|p30|||||||||
32277|Wilpena Pound Sandstone|45022|14|Not recorded|p86|||||||||
39249|Wilson Bluff Limestone Formation|24094|4|Described|p270|Late Eocene|Middle Eocene|Overlies Hampton Sandstone. See Wilson Bluff Limestone. Geological Province: Eucla Basin||||||16-MAR-05
40406|Wilson Bluff Limestone, lower|24606|5|Briefly described|p962 Fig. 6|Middle Eocene|Middle Eocene|Informal - see Wilson Bluff Limestone. Geological Province: Eucla Basin||||||
40406|Wilson Bluff Limestone, lower|61234|4|Described|p6, p7 Fig. 4|Eocene|Eocene|Informal name. Underlain by Hampton Sandstone. Geol. Prov: Eucla Basin. Contact between upper and lower Wilson Bluff Limestone is unconformable.||||||14-MAY-07
40407|Wilson Bluff Limestone, upper|24606|5|Briefly described|p962 Fig. 6|Late Eocene|Late Eocene|Informal - see Wilson Bluff Limestone. Geological Province: Eucla Basin||||||
40407|Wilson Bluff Limestone, upper|61234|4|Described|p6, p7 Fig 4.|Late Eocene|Late Eocene|Informal name. Unconformably underlain by lower Wilson Bluff Limestone; overlain by Nukllarbor Limestone. Geological Province: Eucla Basin. Marine limestone.||||||14-MAY-07
38519|Wilson Bluff carbonate|23488|6|Mentioned|p38 Fig. 4|||Not intended as a formal name - see Wilson Bluff Limestone.  Geological Province: Eucla Basin.||||||
38723|Wilson's Bluff Limestone|24397|6|Mentioned|p237|||Of Singleton (1954). Superseded by Wilson Bluff Limestone.  Geological Province: Eucla Basin.||||||19-FEB-15
38723|Wilson's Bluff Limestone|65942|6|Mentioned|p75|||||||||
38723|Wilson's Bluff Limestone|69386|5|Briefly described|p7|Eocene|Eocene|Eucla Basin.||||Is overlain by Abrakurrie Limestone.|Soft, poorly lithified cool-water carbonate.|
25632|Wilyerpa Quartzite|23818|5|Briefly described|p65|||Underlying unit: Holowilena Ironstone. Of the Yudnamutana Sub-Group.||||||
25632|Wilyerpa Quartzite|29780|6|Mentioned|p32|||||||||
25632|Wilyerpa Quartzite|30799|6|Mentioned|p1|||Stratigraphic relationships with Benda Silstone||||||
25632|Wilyerpa Quartzite|30802|6|Mentioned|p12|||||||||
25632|Wilyerpa Quartzite|32146|6|Mentioned|Fig.3|||||||||
25632|Wilyerpa Quartzite|34269|6|Mentioned|Table 1|||||||||
25632|Wilyerpa Quartzite|34535|6|Mentioned|p65|||Clastic unit||||||
25632|Wilyerpa Quartzite|44659|5|Briefly described|map legend|||Sturtian, lithology.||||||
68760|Wimma Formation|61015|6|Mentioned|p44|Triassic|Triassic|Oil shows.||||||
77511|Wimma Sandstone|62537|6|Mentioned|p191 Fig.2. |Middle Triassic|Middle Triassic|Cooper Basin. Shown as a member of the Arrabury Formation, and has most likely had the rank of Member omitted for reasons of space in the diagram.||||||
37186|Windamere supergroup|23562|6|Mentioned|p294|||Informal.||||||
67973|Windermere Sandstone Member""|44133|6|Mentioned|p145|Aptian|Aptian|||||||
29900|Wingelina Complex""|43052|6|Mentioned|p156|||||||||
74939|Winsanger Basalt|64570|5|Briefly described|p859|Mesozoic|Mesozoic|Misspelling of Wisanger Basalt. Tholeiitic basalt. Age: ranging from 169 to 179Ma (K-Ar). Found on Kangaroo Island, SA.||||||17-FEB-09
23226|Wintinna Formation|43048|6|Mentioned|p24|||||||||
25637|Winton beds|30803|6|Mentioned|p2|||||||||
29157|Winton"" Formation|33939|6|Mentioned|Fig.2|||||||||
72889|Winulta formation|23981|6|Mentioned|p13, p21|Early Cambrian|Early Cambrian|Informal - see Winulta Formation.||||||
38878|Wipajiri Channel Sand|23770|6|Mentioned|p2|Tertiary|Tertiary|Superseded by Wipajiri Formation.||||||
32777|Wipajiri Channel Sands|44223|14|Not recorded|Fig.2||Miocene|Kutjamarpu Fauna.||||||
32778|Wipajiri channel sands|44225|14|Not recorded|p.45,58||Miocene|(H54/5).||||||
35881|Wiperaminga group""|23347|6|Mentioned|p52|||Informal name. Of CEC and Esso Minerals - name now modified to Wiperaminga Subgroup.||||||24-MAR-09
72295|Wiperaminga pelite|62514|6|Mentioned|p747 Fig. 2|||Informal name for psammitic rocks in the Wiperaminga Subgroup (Curnamona Group).  Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
72294|Wiperaminga psammite|62514|6|Mentioned|p747 Fig. 2|||Informal name for psammitic rocks in the Wiperaminga Subgroup (Curnamona Group). Geological Province: Olary Domain/Curnamona Province||||||16-SEP-09
81713|Wire Dam Suite|71129|6|Mentioned|p21|||Geological Province: Gawler Craton. Probable misspelling, see Wire Dam Dolerite p25.||||Intrudes the Broadview Schist.||22-NOV-19
24579|Wirrawilka Beds|24175|6|Mentioned|p9|||||||||
24579|Wirrawilka Beds|37854|6|Mentioned|p10|||||||||
24579|Wirrawilka Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24579|Wirrawilka Beds|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24579|Wirrawilka Beds|40225|3|Fully described|Map sheet|||||||||
24579|Wirrawilka Beds|40294|3|Fully described|p16|||See also P56||||||
24579|Wirrawilka Beds|41403|5|Briefly described|p67|||||||||
24579|Wirrawilka Beds|42222|6|Mentioned|Table 1 P5|||||||||
24579|Wirrawilka Beds|42238|6|Mentioned|p72|||||||||
24579|Wirrawilka Beds|42882|5|Briefly described|Fig.2, P4|||of Callanna Group||||||
24579|Wirrawilka Beds|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
24579|Wirrawilka Beds|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup. Pale grey to buff laminated dolomitic limestone overlying dark grey, finely laminated siltstone, locally silicified.||||||
24579|Wirrawilka Beds|72492|5|Briefly described|p2 Fig.1 , p2|Neoproterozoic|Neoproterozoic|In the Worumba Anticline.||Curdimurka Subgroup||Underlies Niggly Gap Beds.|Includes stromatolites.|
24579|Wirrawilka Beds|73222|6|Mentioned|p7|Tonian|Tonian|Flinders Ranges. Torrensian.||Curdimurka Subgroup, Callanna Group, Warrina Supergroup||Unconformably overlain by Niggly Cap Beds. Possibly equivalent to Dunns Mine Limestone and Rook Tuff.||
34334|Wirrda breccias|22629|6|Mentioned|p160|||||||||
37138|Wirrda suite|23563|6|Mentioned|p214|||||||||
67975|Wirrealpa Limestone, lower|44133|6|Mentioned|p28|||||||||
67974|Wirrealpa Limestone, upper|44133|6|Mentioned|p28|||||||||
24580|Wirreanda Dolomite Beds|22889|6|Mentioned|p33|Adelaidean|Adelaidean|Parent - Emeroo Subgroup.  Former Parent Unit - River Wakefield Subgroup, see p33 for details on change.||||||
24580|Wirreanda Dolomite Beds|37854|6|Mentioned|Table 1|||||||||
24580|Wirreanda Dolomite Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24580|Wirreanda Dolomite Beds|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Torrensian||||||
24580|Wirreanda Dolomite Beds|40225|4|Described|Map sheet|||||||||
24580|Wirreanda Dolomite Beds|40294|3|Fully described|p33|||||||||
24580|Wirreanda Dolomite Beds|41404|4|Described|p92|||||||||
24580|Wirreanda Dolomite Beds|42222|6|Mentioned|p13|||||||||
24580|Wirreanda Dolomite Beds|43052|5|Briefly described|p177,Table 6.1|||of River Wakefield Subgroup||||||
24580|Wirreanda Dolomite Beds|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the River Wakefield Subgroup. Blue-grey dolomite with tepee structures; dolomitic sandstone, siltstone; minor magnesite conglomerate.||||||
39215|Wistow Bluestone|23731|6|Mentioned|p27|||Of Tapanappa Formation. Commercial name for quarried 'bluestone' rock.||||||
39215|Wistow Bluestone|61237|5|Briefly described|p36|Cambrian|Cambrian|Building stone quarried from the Tapanappa Formation for walling and paving stone.||||||16-AUG-05
29159|Witchelina Quartzite""|37854|6|Mentioned|p14|||||||||
25640|Witchelina quartzite""|37854|6|Mentioned|p14|||||||||
27619|Wockerawirra Dolomite Member|22510|5|Briefly described|table1p37|||Age: Sturtian. Central Flinders Ranges||||||
27619|Wockerawirra Dolomite Member|32510|6|Mentioned|p106|||||||||
27619|Wockerawirra Dolomite Member|39344|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
27619|Wockerawirra Dolomite Member|41405|3|Fully described|p165|||||||||
27619|Wockerawirra Dolomite Member|42882|5|Briefly described|p9, Table 1 p3|||of Tapley Hill Formation||||||
27619|Wockerawirra Dolomite Member|43052|5|Briefly described|p189,Table 6.1|||of Tapley Hill Formation||||||
27619|Wockerawirra Dolomite Member|43845|6|Mentioned|Fig 5 p45||Neoproterozoic|Member of Tapley Hill Formation||||||12-JUL-16
27619|Wockerawirra Dolomite Member|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tapley Hill Formation. Limestone, dolomitic siltstone, silty dolomite.||||||
27619|Wockerawirra Dolomite Member|64846|6|Mentioned|p208 Fig.11 |Cryogenian|Cryogenian|Rank not shown in diagram.||||||
27619|Wockerawirra Dolomite Member|67979|6|Mentioned|p531 Fig.2|Marinoan|Marinoan|This article describes a disconformity between Wockerawirra Dolomite and underlying Tapley Hill Formation (p543), and seems to propose that the Wockerawirra Dolomite be reduced to become the basal member of the overlying Sunderland Formation (Upalinna Subgroup). See Wockerawirra Dolomite.||Sunderland Formation||||22-SEP-14
27619|Wockerawirra Dolomite Member|70407|5|Briefly described|p103 Fig 2|Neoproterozoic|Neoproterozoic|Age: Sturtian.||Of Tapley Hill Formation.||||
27619|Wockerawirra Dolomite Member|72449|6|Mentioned|p1||||||||Includes flaggy dolomite. Included only pn p1.|
29161|Wollongbar Clay Loam|39019|6|Mentioned|p380|||||||||
34226|Wombat Member|22663|5|Briefly described|S97-1 and 2 p3|||||||||
83534|Wonga-Moola Supersuite|73525|6|Mentioned|p19 Fig.13|||||||||
72281|Wonoka Formation, upper|24586|5|Briefly described|p51|Adelaidean|Adelaidean|Informal - see Wonoka Formation. Intertongues with Bonney Sandstone. Geological Province: Adelaide Geosyncline.||||||
37125|Wonoka formation|23562|6|Mentioned|p294|||Informal.||||||
37125|Wonoka formation|23806|6|Mentioned|p1131|||Informal - see Wonoka Formation.||||||
75620|Woodendinna Limestone|65313|6|Mentioned|p576 Fig.5|Cambrian|Cambrian|Probable mis-spelling of Woodendinna Dolomite.||||||26-MAR-12
37130|Woodnamoka Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|Possible misspelling of Woodnamoka Phyllite.||||||
73834|Woodnamoka phyllite|24546|5|Briefly described|p2 - 6 Tb.1|||Informal. Fine grained sandy schist.||||||07-JAN-10
40462|Woodnamooka Phyllite|24593|5|Briefly described|p613 Fig. 1b|||Of the Burra Group.  Geological Province: Mount Painter Inlier.||||||
25649|Wooldridge Limestone""|41088|6|Mentioned|p141|||||||||
29173|Woolshed Flat shale|41526|6|Mentioned|p36|||||||||
31856|Woolshed Granite|45003|6|Mentioned|p57|||Invalid name||||||
78178|Wooltana Basalt|68822|5|Briefly described|p322|Cryogenian|Tonian|Possible open ocean depositional environment. Occurs at the base of the Adelaide Rift Complex.|~830 +/- 50 Ma, Rb-Sr (Compston et al. 1966)|||||
37136|Wooltana Basalts|23562|6|Mentioned|p299|||||||||
37136|Wooltana Basalts|23932|6|Mentioned|p668|Neoproterozoic|Neoproterozoic|||||||
79558|Wooltana Formation|67870|5|Briefly described|p9|Neoproterozoic|Neoproterozoic|Adelaide Rift System.||Arkaroola Subgroup.||||
30497|Wooltana Volcanic suite|43190|6|Mentioned|p29|||Informal name. Callanna Group.||||||
37135|Wooltana basalts|23562|6|Mentioned|p299|||Informal.||||||
27941|Woomera Shale Member|22649|6|Mentioned|p 143|||equivalent to the Brachina Formation p 143.  Province - Stuart Shelf in the Western Adelaide Geosyncline.||||||
27941|Woomera Shale Member|23287|6|Mentioned|Fig.2|||Age: Lower Ediacarian. of Stuart Shelf.||||||
27941|Woomera Shale Member|30807|6|Mentioned|p102|||Suggested map symbol||||||
27941|Woomera Shale Member|31540|4|Described|p10|||||||||
27941|Woomera Shale Member|37461|6|Mentioned|Table 5.I|||||||||
27941|Woomera Shale Member|37932|6|Mentioned|p546|||||||||
27941|Woomera Shale Member|38157|6|Mentioned|p267|||||||||
27941|Woomera Shale Member|40448|5|Briefly described|p38|||||||||
27941|Woomera Shale Member|41005|6|Mentioned|p420|||||||||
27941|Woomera Shale Member|41429|6|Mentioned|p223|||||||||
27941|Woomera Shale Member|42469|6|Mentioned|p24|||Andamooka SH53-12||||||
27941|Woomera Shale Member|42723|5|Briefly described|map legend|Marinoan||||||||
27941|Woomera Shale Member|43048|4|Described|Table 1.|||||||||
27941|Woomera Shale Member|43052|6|Mentioned|p192,table 6.1|||Synonym for Tregolana Shale Member||||||
27941|Woomera Shale Member|43094|6|Mentioned|p35|||||||||
27941|Woomera Shale Member|44689|14|Not recorded|map legend||Late Adelaidean|Andamooka. (H53-12). Member of Tent Hill Formation. Upper Adelaidean.||||||
27941|Woomera Shale Member|44934|5|Briefly described|Map Legend||Adelaidean|||||||
27941|Woomera Shale Member|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Tent Hill Formation. Equivalent to Tregolana Shale Member. Laminated red, brown and green shales. Partly micaceous.||||||
27941|Woomera Shale Member|61732|5|Briefly described|p42|||Regarded as synonymous with Tregalona Shale Member (Preiss (1987). Geological Province: northern Stuart Shelf.||||||07-FEB-11
27941|Woomera Shale Member|70406|5|Briefly described|p117|||Obsolete name of Johns (1968). Northern Stuart Shelf. Lateral equivalent of Tregolana Shale.||||||
81633|Woomera Shale''|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Woomera area. Of Adelaide Geosyncline.||Unit of Wilpena Group.||Equivalent to Tregolana Shale Member. Overlain by Corraberra Sandstone Member. Underlain by Nuccaleena Formation.||16-SEP-19
81633|Woomera Shale''|73227|6|Mentioned|p25|||[Written as 'Woomera Shale']. Woomera area.||Wilpena Group||Underlain by Nuccaleena Formation. Overlain by Corraberra Sandstone Member. Equivalent to Tregolana Shale Member.||
34895|Woorawoora Formation|22907|6|Mentioned|41|||Probable misspelling of Woora Woora Formation. Parent Disappointment Group||||||
37128|Wortupa Formation|23562|5|Briefly described|p295 Fig 2|Cryogenian|Cryogenian|||||||
24585|Worumba Dolomite Beds|24175|6|Mentioned|p9|||Of the Worumba Anticline (Forbes et al, 1981).||||||
24585|Worumba Dolomite Beds|37854|6|Mentioned|p13|||||||||
24585|Worumba Dolomite Beds|39344|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24585|Worumba Dolomite Beds|39348|6|Mentioned|Map legend|Adelaidean|Adelaidean|Willouran||||||
24585|Worumba Dolomite Beds|40225|4|Described|Map sheet|||||||||
24585|Worumba Dolomite Beds|40294|3|Fully described|p26|||See also P58||||||
24585|Worumba Dolomite Beds|41403|5|Briefly described|p68|||||||||
24585|Worumba Dolomite Beds|42222|6|Mentioned|Table 1 P5|||||||||
24585|Worumba Dolomite Beds|42238|6|Mentioned|p72|||||||||
24585|Worumba Dolomite Beds|42882|5|Briefly described|Fig.2, P4|||of Callanna Group||||||
24585|Worumba Dolomite Beds|43052|5|Briefly described|p175,Table 6.1|||of Curdimurka Subgroup.||||||
24585|Worumba Dolomite Beds|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Curdimurka Subgroup. Upper and lower members of pale grey to buff, laminated dolomite seperated by siltstone.||||||
82037|Worumba Shale Member|72492|5|Briefly described|p3, p6-9, p10-11|Neoproterozoic|Neoproterozoic|Of the Worumba Dolomite? Also shown as Worumba Shale p6. See also p11 Tb.3, p11, p13-14 Tb.4, p15 Fig.9b, p16 Fig.10a, p16-17. Coordinates are provided.|||||Includes plane-laminated silty shales, often with alternating silt and shale laminae and stromatolitic carbonate with nodular gypsum or anhydrite pseudomorphs.|16-SEP-20
27019|Wright Hill beds|23282|6|Mentioned|p52,58,59|||Lower part may be equivalent to Alinya Formation.||||||
27019|Wright Hill beds|23287|6|Mentioned|Fig.2,4|||Age: Ediacarian. of Eastern Officer Basin.||||||
27019|Wright Hill beds|23288|6|Mentioned|Fig.5,18|||of Central Officer Basin.||||||
27019|Wright Hill beds|36701|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27019|Wright Hill beds|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Siltstone, sandstone, quartzite, chert.||||||
27019|Wright Hill beds|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Siltstone, sandstone, quartzite and chert. Age and correlation very uncertain.||||||
27019|Wright Hill beds|61732|6|Mentioned|p63, p68|||Geological Province: Birksgate Sub-basin.||||||07-FEB-11
27019|Wright Hill beds|62453|5|Briefly described|p5 Fig. 3, 18|Cryogenian|Cryogenian|Geological Province: Officer Basin. Lateral equivalent to Lefroy Formation.||||||03-FEB-14
27019|Wright Hill beds|63397|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|||||||18-JUL-07
27019|Wright Hill beds|64103|6|Mentioned|p400 Fig. 3|Cryogenian|Cryogenian|Geological Province: Officer Basin.||||||07-FEB-11
27019|Wright Hill beds|67536|6|Mentioned|Map Legend|||One of several Formations mapped collectively as N2.|||||Dominantly marine shale, siltstone, sandstone and limestone.|
27019|Wright Hill beds|67921|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown only in section and grouped with Punkerri Sandstone, Ungoolya Group (Rodda beds), Karlaya Limestone. Group description: Marine sandstone, grey indurated mudstone and limestone.||Ungoolya Group||Said to be equivalent to Wilpena Group||
27019|Wright Hill beds|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|E Officer Basin.||||||
27019|Wright Hill beds|73100|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
27019|Wright Hill beds|73109|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
27019|Wright Hill beds|73111|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Subsurface.||||Equivalent to Wilpena Group.||
30614|Wudinna Granite|65390|5|Briefly described|p26 Tb.1|Calymmian|Calymmian|Of Hiltaba Suite. Pinkish, coarse-grained granite-adamellite, minor porphyritic varieties and minor aplite dykes. Aged 1519 +/- 67 Ma (Rb-Sr: Webb et al., 1986).||||||26-FEB-15
41714|Wudinna granite|24197|5|Briefly described|p75 Tb. 8.1|Mesoproterozoic|Mesoproterozoic|Informal name. Of the Kokatha suite. Age: 1592Ma.||||||07-FEB-11
41714|Wudinna granite|50605|5|Briefly described|p(ii), 1.3, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Gawler Craton & Curnamona Province. Of the Kokatha suite.||||||
77777|Wundowie Limestones|67180|6|Mentioned|p608, p609|Cryogenian|Cryogenian|Collective reference to Wundowie Limestone #1, #2, and #3. ||Unit in Enorama Shale||||
82113|Wynbring granite|72459|5|Briefly described|p22|Palaeoproterozoic|Palaeoproterozoic|Christie Subdomain of the Gawler Craton. Interpreted to be of the Ifould Magmatic event.|1669 +/- 10 Ma (Teasdale, 1997)|||||
73969|Wynbring granite""|61556|5|Briefly described|p9-10  Figure|Carpentarian|Carpentarian|In Central Province - Mount Christie.||||||21-NOV-07
29179|Wywyana dolomite|30028|6|Mentioned|p375|||Refs Coats 1973||||||
24591|Yadlamalka Formation|38926|2|Defined|p34|Late Precambrian|Late Precambrian|||||||
24591|Yadlamalka Formation|41404|4|Described|p99|||Mention P98||||||
24591|Yadlamalka Formation|42236|5|Briefly described|p107|||||||||
24591|Yadlamalka Formation|42238|6|Mentioned|p73|||||||||
29180|Yakaninna Formation|34175|6|Mentioned|p36|||||||||
40175|Yanac picrites|24599|5|Briefly described|p498|Neoproterozoic|Neoproterozoic|Informal name.||||||
78501|Yankaninna Formation, lower|67979|4|Described|p534 Fig.5, p543-545|Marinoan||Informal subdivision. Presented as Lower Yankaninna Formation in figures.||Yankaninna Formation||Is overlain by informal Yankaninna Formation, Upper; the Wockerawirra Dolomite (base of Sunderland Formation) is considered a lateral, time-equivalent succession.|Finely laminated, steel grey limestone horizons interbedded within host calcareous silty-shales|22-SEP-14
78502|Yankaninna Formation, upper|67979|4|Described|p534 Fig.5, p536, p544 Fig.11, p545|Marinoan||Informal subdivision. Presented as Upper Yankaninna Formation in figures.||Yankaninna Formation||Overlies informal Yankaninna Formation, Lower; overlain conformably/gradationally by Amberoona Formation and Enorama Shale; Sunderland Formation is considered a time-equivalent succession.|Calcareous siltstones containing coarser sandy interbeds|22-SEP-14
26289|Yannabie Rhyodacite|24346|6|Mentioned|p111 App 1, p98 Fig.1|||Supserseded by Eucarro Rhyolite Formation.||||||
26289|Yannabie Rhyodacite|24474|5|Briefly described|p36 Fig. 1|||Of the Gawler Range Volcanics.  Geological Province: Gawler Craton.||||||
26289|Yannabie Rhyodacite|40430|2|Defined|p4|Mesoproterozoic|Mesoproterozoic|||||||
26289|Yannabie Rhyodacite|41619|6|Mentioned|Map legend|Mesoproterozoic||||||||
26289|Yannabie Rhyodacite|42283|6|Mentioned|Fig.5 P82|||||||||
26289|Yannabie Rhyodacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26289|Yannabie Rhyodacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26289|Yannabie Rhyodacite|43052|5|Briefly described|p111|||of Gawler Range Volcanics||||||
26289|Yannabie Rhyodacite|65922|5|Briefly described|p17 Tb. 2, p18-19, 21|Calymmian|Calymmian|Of Gawler Range Volcanics. Subsequently included in Eucarro Rhyolite. Non-porphyritic and porphyritic rhyodacite grading to rhyolite with phenocrysts of plagioclase, K-feldspar and quartz. Intensely weathered and poorly exposed. Overlies Nonning Rhyodacite and Eucarro Dacite; underlies and intruded by Paney Rhyolite. Up to 100m thick.||||||
26289|Yannabie Rhyodacite|67028|5|Briefly described|p362, p364 Tb.1|Calymmian|Calymmian|Information on magnetic characteristics presented. Described as Roxby Downs-type p362, but shown as Kokatha-type in Table 1.||Gawler Range Volcanics||||24-APR-12
26289|Yannabie Rhyodacite|72459|6|Mentioned|p47|||||||||
38171|Yannabie Rhyodacite""|24346|4|Described|p99, 102|||Now mapped as Eucarro Rhyolite.||||||
80114|Yannabie Rhyolite|68158|5|Briefly described|p4|||||Gawler Range Volcanics.|||Amygdaloidal, vesicular rhyolite; abundant free quartz, top of flow.|
26241|Yantea Rhyodacite|24474|3|Fully described|p41|||Of the Glyde Hill Volcanic Complex.  Max. thickess: 150m.  Geological Province: Gawler Craton.||||||
26241|Yantea Rhyodacite|30984|2|Defined|p11|Proterozoic|Proterozoic|||||||
26241|Yantea Rhyodacite|40430|6|Mentioned|p7|||||||||
26241|Yantea Rhyodacite|41974|6|Mentioned|p411|||||||||
26241|Yantea Rhyodacite|42546|5|Briefly described|Map legend|Mesoproterozoic||||||||
26241|Yantea Rhyodacite|42721|5|Briefly described|map legend|Carpentarian||||||||
26241|Yantea Rhyodacite|42722|5|Briefly described|map legend|Carpentarian|Carpentarian|Of the Glyde Hill Volcanic Complex.  Reddish-brown porphyritic rhyodacite grading to dacite locally; phenocrysts of pink K-feldspar  and some cream-coloured plagioclase up to about 10mm long.||||||07-APR-05
26241|Yantea Rhyodacite|42736|5|Briefly described|map legend|Mesoproterozoic||||||||
26241|Yantea Rhyodacite|43052|5|Briefly described|p111|||of Glyde Hill Volcanic Complex||||||
26241|Yantea Rhyodacite|43071|4|Described|p15,Table 2|||of Gawler Range Volcanics||||||
26241|Yantea Rhyodacite|43094|4|Described|table 4.|||of Glyde Hill Volcanic Complex||||||
26241|Yantea Rhyodacite|67909|5|Briefly described|p127-128, 130-131, 140|Mesoproterozoic|Mesoproterozoic|Lake Everard area. Appears in text as Yantea Rhyolite-dacite. Total volume is ~170 km3. Volcanic textures and emplacement mechanism tabulated.||Glyde Hill Volcanic Complex.|||Includes autobreccia zones. Locally peperitic at base.|
26241|Yantea Rhyodacite|69649|5|Briefly described|p17, p24-25|Mesoproterozoic|Mesoproterozoic|Giles (1977). Locally occupies paleovalleys within older units. Up to 150m thick. Shows prominent flow layering, and several layers up to 3m thick of spherulites.||Unit in Glyde Hill Volcanic Complex.||Is overlain conformably by Whyeela Dacite.|Massive, brick red, porphyritic rhyodacite grading to dacite, containing coarse phenocrysts of K-feldspar and chlorite (after clinopyroxene) in a devitrified, limonite-stained matrix.|26-FEB-15
38634|Yardea Dacite Formation|24346|3|Fully described|p111 Appendix 1|||Now includes Pondanna and Moonaree Dacite Members.  Referred to as Yardea Dacite throughout text. Underlain by Eucarro Rhyolite Formation.||||||
38634|Yardea Dacite Formation|72065|6|Mentioned|p106|||Geological province: Gawler Craton. Informal/Misspelt use: See Yardea Dacite.||||||
38639|Yardea Dacites|24346|6|Mentioned|p109|||Misspelt - see Yardea Dacite.||||||
78853|Yardina Claystone|66131|5|Briefly described|p242 Fig.2, p243|Miocene|Miocene|Said to be "also regarded as member of the Etadunna Formation". Age from Fig.2 - stratigraphic correlation chart.||||||
25665|Yarra-wurta Shale|36966|6|Mentioned|Fig.1|||Variation of Yarrawurta?||||||
25665|Yarra-wurta Shale|64696|5|Briefly described|p133 Fig.14|Cambrian|Cambrian|||||||
75588|Yarrah Beds|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Wilson - Quorn area.||||Overlies Pound Sandstone.||18-FEB-11
32469|Yellow Polyzoal Bed""|34308|6|Mentioned|p198|||Occurs between Wilson Bluff Limestone and Nullarbor Limestone.||||||
32469|Yellow Polyzoal Bed""|65942|6|Mentioned|p74|||||||||
81634|Yeltacowie Sandstone''|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Torrens Hinge Zone. Of Adelaide Geosyncline.||||Overlain by Nue Sandstone. Underlain by Pandurra Formation.||16-SEP-19
76822|Yeralina Subgroup|67030|5|Briefly described|p409 Fig. 2|Cryogenian|Cryogenian|[Mis-spelling of Yerelina Subgroup].|||Includes unnamed siltstone, Grampus Quartzite, Pepuarta Tillite, Gumbowie Arkose.|Overlies Enorama Shale, underlies Nuccaleena Formation and Seacliff Sandstone; shown as equivalent to Elatina Formation.||26-APR-12
77403|Yerelia Subgroup|65376|6|Mentioned|p140 Fig.4.22.|Neoproterozoic|Neoproterozoic|||||||
29191|Yerelina Sub-group|30376|6|Mentioned|p75|||||||||
29191|Yerelina Sub-group|36833|6|Mentioned|Fig.1|||||||||
75769|Yerila granite|65455|6|Mentioned|p9|Mesoproterozoic|Mesoproterozoic|See Yerila Granite, p12.||||||09-MAY-12
73145|Yorke Peninsula Limestone|63222|5|Briefly described|p40, p41|||Trade name for a dimension stone from a stone quarry at Coobowie, Yorke Peninsula; the limestone unit is known as Coobowie Limestone.||||||01-MAR-10
36880|Younger Granite Suite""|23394|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
36880|Younger Granite Suite""|23818|6|Mentioned|p36 Fig.9|||||||||
36880|Younger Granite Suite""|61523|5|Briefly described|p8|||Informal name. Granites, granodiorites, leucogranites and pegmatites. Geological Province: Mount Painter Inlier.||||||
82114|Yudnamatana gneiss|72459|6|Mentioned|p69|||Informal term originally of Paul (1998), termed the Hot Springs gneisses by Neumann (1996).||||||
81714|Yudnapinna Beds''|71129|4|Described|p107,110-111,114,116-118,208|Cryogenian|Cryogenian|Of Stuart Shelf. Deposited during ensuing glacio-eustatic sea-level rise after Sturt Glaciation. Transgressive-regressive siliciclastic sequence, informally named by exploration geologists working in the SIX MILL HILL area. Reaches a maximum thickness of 91.5m as intersected in drillhole PACMINEX EX 37 in SIX MILE HILL.||Unit of Upalinna Subgroup.||Overlain by Whyalla Sandstone. Underlain by Augusta Shale where present, or Tapley Hill Formation or Pandurra Formation or Gawler Range Volcanics. Equivalent to Wilmington Formation.|Fine-grained sandstones and siltstones.|
29919|Yudnapinna beds""|43052|5|Briefly described|Table 6.1|||Of Willochra Subgroup?||||||
29919|Yudnapinna beds""|72247|5|Briefly described|p41,43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline. Nomenclature of Tonkin 1974a, b.||||Underlain by Tapley Hill Formation.||
36097|adamellite 36097|43052|5|Briefly described|Table 5.6 p129|Mesoproterozoic|Mesoproterozoic|Coarse-grained granite, adamellite and granodiorite. Various ages from 1583 to 1282 Ma, various methods.||||||
36043|aplite 36043|44535|6|Mentioned|map legend||Proterozoic|Unnamed unit used in Proterozoic Granites GIS. Desc: Aplite of Indulkana Shear Zone.||||||
33881|bimba suite|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill Olary Domain||||||
38630|black (Yardea) Dacite""|24346|5|Briefly described|p103|||Orginally mapped by Blissett (1975) as an informal unit of Yardea Dacite, part npw mapped as Mount Double Ignimbrite.||||||
38629|black Yardea Dacite|24346|5|Briefly described|p98 Fig.1, p99|||Informal unit of Yardea Dacite.  Now mapped as Pondanna and Moonaree Dacite Members.||||||
38629|black Yardea Dacite|24474|5|Briefly described|p36  Fig. 1|||Referred to as basal black Yardea Dacite in figure.  Informal name - see Yardea Dacite.   Geological Province: Gawler Craton.||||||
33882|calc - silicate suite|22463|5|Briefly described|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Olary Domain||||||
40453|calc-silicate Suite|24592|6|Mentioned|p634|||Of the Willyama Supergroup. Geological Province: Curnamona Province. Infomal form of the informal Calc-silicate Suite.||||||
73831|ediacara member|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Informal. Of Rawnsley Quartzite. Geological Province: Adelaide Fold Belt.||||||10-JAN-08
36006|gneiss 36006|40911|6|Mentioned|Map legend||Proterozoic|Foliated feldspar-quartz-biotite and quartz-biotite gneiss of granitic and adamellitic composition||||||
36041|gneiss 36041|31698|6|Mentioned|Map legend||Proterozoic|Unnamed unit for Proterozoic Granites GIS. Desc: Biotite hornblende gneisses: Light and dark grey medium granined biotite and hornblende gneiss with rare schist bands (upper amphibolite facies), some ptygmatic folding. Well foliated augen gneiss in JWA.||||||
36042|granite 36042|31698|6|Mentioned|Map legend||Proterozoic|Unnamed unit for Proterozoic Granites GIS. Desc: Undifferentiated aplitic granites and granitic rocks: Massive light red-weathering porphyritic microgranite, gneissic granite porphyry, massive to slightly gneissic fine and medium grained granites...||||||
36091|granite 36091|43052|5|Briefly described|Table 5.6 p128|Mesoproterozoic|Mesoproterozoic|Unnamed unit. Homogeneous, coarse-grained red granite. Various ages given between 1581 and 1361 Ma.||||||
36092|granite 36092|43052|5|Briefly described|Table 5.6 p128|Mesoproterozoic|Mesoproterozoic|Unnamed unit. Leucocratic pink, medium to coarse-grained granite to adamellite, including some porphyritic varieties. Age: 1478+/-38 Ma, Rb-Sr.||||||
36093|granite 36093|43052|5|Briefly described|Table 5.6 p128|||Unnamed unit. Bimodal suite of fine to coarse-grained and porphyritic granite (high SiO2) and syenite to granodiorite (low SiO2).||||||
36094|granite 36094|43052|5|Briefly described|Table 5.6 p128|||Unnamed unit. Age: 1474+/-45 Ma, Rb-Sr. Coarse-grained (~5mm) red granite and adamellite in Tarcoola DDH1-3.||||||
36095|granite 36095|43052|5|Briefly described|Table 5.6 p129|Mesoproterozoic|Mesoproterozoic|Unnamed unit. Medium-grained pinkish granite, adamellite and granodiorite. Age: 1475 +/-45 Ma, Rb-Sr.||||||
36096|granite 36096|43052|5|Briefly described|Table 5.6 p129|||Unnamed unit. Red, coarse-grained granite.||||||
35721|intrusives 35721|43052|6|Mentioned|p150|Mesoproterozoic|Mesoproterozoic|Included with undifferentiated quartzofeldspathic schist and gneiss.||||||
34863|lower Blanche Point Formation|23010|6|Mentioned|p339|||||||||
35083|lower Boorthanna Formation|23054|6|Mentioned|p17|||||||||
35087|lower Bulldog Shale|23054|6|Mentioned|p24|||||||||
34690|lower Lake Frome Group|22858|6|Mentioned|p92|||||||||
35089|lower Oodnadatta Formation|23054|6|Mentioned|p27|||||||||
37478|older granite suite|24045|6|Mentioned|p533 Fig.2|||Informal name.||||||
33880|pelite suite|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill - Olary Domain||||||
33892|quartzo feldspathic suite|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Geol province Olary Domain||||||
75841|upper Namur Sandstone""|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Informal name for upper part of Namur Sandstone above unconformity and overlying Westbourne Formation. Quartz-rich sediment. See Namur Sandstone.||||||08-MAR-12
75841|upper Namur Sandstone""|72297|6|Mentioned|p742|||Eromanga Basin. Petroleum reservoir.||||||
35090|upper Willawortina Formation|23054|6|Mentioned|p30|Pleistocene|Early Pleistocene|||||||
75842|uppermost Westbourne Formation""|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Informal name for earliest Cretaceous rocks in NE Qld and overlying Westbourne Formation proper. Quartz-rich sediment.||||||
