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
31|Abels Bay formation|41895|5|Briefly described|p11|||||||||
45|Aberfoyle Group|41141|6|Mentioned|p295|||||||||
30086|Ables Bay Formation|43084|5|Briefly described|p93|||Misspelling of Abels Bay Formation.||||||20-MAR-07
93|Adam's Beds|42838|5|Briefly described|Table 1 P377|||Misspelling/old form of Adams beds?||||||
102|Adamsfield Beds|39235|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
102|Adamsfield Beds|41793|6|Mentioned|p45|||See also p63.||||||20-MAR-07
102|Adamsfield Beds|69874|6|Mentioned|p134, p135 Fig 4.33|Late Cambrian|Late Cambrian|Adamsfield Ultramafic Complex was tectonically emplaced and exposed to erosion before deposition of Adamsfield Beds, which containe ultramafic detritus and Late Cambrian (Idamean) fossils.||Denison Group||||
28317|Adamsfield Ultramafic Complex|37056|6|Mentioned|p498|||||||||
28317|Adamsfield Ultramafic Complex|41594|6|Mentioned|p53|||||||||
28317|Adamsfield Ultramafic Complex|41793|6|Mentioned|p63|||||||||
28317|Adamsfield Ultramafic Complex|42227|6|Mentioned|p56|Cambrian|Cambrian|Ultramafic rocks.||||||16-JUN-09
28317|Adamsfield Ultramafic Complex|44135|6|Mentioned|p38|||||||||07-DEC-09
28317|Adamsfield Ultramafic Complex|69874|4|Described|p104 Fig 4.8, p107, p110 Fig 4.11, p117|Early Cambrian|Early Cambrian|See also p119 Table 4.2, p125-126, p134-136, p185. Brown et al. (1972, 1989). A series of blocks largely within and sitting on the Ragged Basin Complex. Shown as Adamsfield UC in Fig 4.11 and as Adamsfield Ultramafics on p107. Arcuate belt about 15km long and up to 1.4km wide on western flank of Sawback Ridge. Tectonically emplaced and exposed to erosion before deposition of Adamsfield Beds. Subsequently re-emplaced into core of large anticline of Ordovician strata during Middle Devonian Tabberabberan Orogeny. Lithology described in some detail.||Ragged Basin Complex||Within and on Ragged Basin Complex. To south, Adamsfield UC passes into melange at eastern margin of Ragged Basin Complex. Eastern Margin faulted against Denison Group.|Consists almost entirely of partly serpentinised dunite, olivine orthopyroxenite and orthopyroxenite. Ultramafics - layered dunite and harzburgite, layered pyroxenite and dunite; volcanics - boninite (high Mg andesite), low Ti tholeiite.|
104|Adamsfield complex|41594|4|Described|p25|||[Originally entered for Qld. CEBMar95]||||||
104|Adamsfield complex|41793|6|Mentioned|p63|||||||||
104|Adamsfield complex|42838|5|Briefly described|p374|||||||||
135|Adit Knob porphyry|35844|6|Mentioned|p53|||||||||
73641|Akaroa Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith. I-type granite, felsic, unfractionated, reduced. Name implied from map legend.||||||
73641|Akaroa Granite|71100|6|Mentioned|p126|||||||||
73641|Akaroa Granite|71141|6|Mentioned|p126|||||||||
73641|Akaroa Granite|71730|6|Mentioned|p33, p35, p37, p43, p56|||[Formal name intended? Name only implied by tables].|||||I-type granite.|
73251|Amber slate|63244|6|Mentioned|p1|||||||||08-MAY-07
411|Anchor Granite|37797|6|Mentioned|Fig.1|||||||||
411|Anchor Granite|61216|5|Briefly described|p43|||Alkali feldspar granite of the Lottah Pluton.  Hosts the Anchor tin mine in the greisenised top section of the granite.  Intrudes the Poimena Pluton - both granite bodies being part of the Blue Tier Batholith.||||||10-FEB-11
411|Anchor Granite|61723|6|Mentioned|p815|||Also known as Lottah Granite.||||||18-SEP-07
411|Anchor Granite|65646|6|Mentioned|p39.|||Also called Lottah Pluton. Alkali feldspar granite intruding Poimena Pluton. Both are part of Blue Tier Batholith.||||||09-JAN-15
412|Anchor granite|37797|6|Mentioned|p139|||||||||
421|Anderson's Creek complex|41594|6|Mentioned|p27|||||||||
35647|Andersons Creek Mafic-Ultramafic Complex|23114|5|Briefly described|p468||Cambrian|||||||
83244|Andersons Creek Ultrabasic Complex|73369|6|Mentioned|p320, p332|||Encloses the Settlers Metamorphosed Greywacke. Cambrian?|||||Serpentinite.|
81361|Animal Creek Graywacke|70274|6|Mentioned|p463|||Associated with mafic-felsic magmatism and the Que-Hellyer Volcanics?||||||
26347|Ansons Bay Adamellite|35825|6|Mentioned|p166|||||||||
26347|Ansons Bay Adamellite|39677|6|Mentioned|Map legend|Devonian|Devonian|||||||
26347|Ansons Bay Adamellite|61723|6|Mentioned|p813 Fig. 4|||Same unit as Ansons Bay Granite, but probably superseded by it?|SHRIMP age 384.3 +/-2.4 Ma|||||21-DEC-09
473|Ansons Bay North Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Ansons Bay Adamellite. NOT var. on Ansons Bay South Granite.||||||
474|Ansons Bay South Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Ansons Bay Adamellite. NOT var. on Ansons Bay North Granite.||||||
475|Ansons Bay adamellite|39927|6|Mentioned|p305|||||||||
476|Ansons Bay biotite-garnet adamellite|39927|6|Mentioned|p311|||||||||
74912|Anthony Road andesite|64395|5|Briefly described|p172|||Informal name. Hornblende-phyric andesite occurring mainly as intrusives within the upper part of southern Central Volcanic Complex; together with Reservoir and Crown Hill andesites these  form Suite 2 of Mount Read Volcanics.||||||07-FEB-11
74912|Anthony Road andesite|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Central Mount Read Volcanics, with U-Pb SHRIMP zircon age of 502.2+\-7 Ma, and Ar-Ar hornblende age of 501.5+\-14 Ma.|c. 501 Ma|||||
505|Applebee "Volcanics"|31475|6|Mentioned|p82|||||||||
40000|Archer Subgreywacke and Slate|24548|5|Briefly described|p5 Fig.I, p6 Fig.II|Cambrian|Cambrian|Of the Dundas Group. Informal compound name - see Archer Formation. See also Golden Valley Map 4687.||||||20-MAR-07
28333|Arm Bridge Rhythmites|30524|6|Mentioned|Table 2|Pleistocene|Pleistocene|Lithostratigraphical relationships.||||||04-AUG-08
74373|Arndell Formation|63170|6|Mentioned|p227|||Probably misspelt? See Arndell Sandstone.||||||07-FEB-11
74373|Arndell Formation|69875|6|Mentioned|p256 |Silurian|Ordovician|Florentine Valley. Used possibly interchangeably with Arndell Sandstone (references p243 Fig 5.2, p244, p256-258, p263).||||||
621|Arndell Sandstone Formation|41954|6|Mentioned|Table 1 P12|||||||||
34462|Arthur Metamorphics|22705|6|Mentioned|Fig.2 p791|||Informal name - probably refers to rocks of the Arthur Metamorphic Complex.||||||02-JUL-08
649|Arthur River Sequence""|41795|6|Mentioned|p34|||||||||
73449|Arthur River Sequences""|63168|6|Mentioned|p57|||Of Groves (1968). Informal name. In Cleveland-Waratah area.||||||
40001|Ashley basalt|24548|6|Mentioned|p10|Tertiary|Tertiary|Informal - see Ashley Basalt.||||||21-MAR-07
24674|Austral Creek Formation|41795|4|Described|p63|||||||||
24674|Austral Creek Formation|41896|6|Mentioned|p27|||Same as Austral Creek Siltstone.||||||05-AUG-08
30392|Back Peak Beds|43131|5|Briefly described|p569, 576|||Should be Back Peak beds.||||||
30392|Back Peak Beds|69874|5|Briefly described|p157|Drumian|Drumian|Fossey Mountains area.||Eastern Quartz-Phyric Sequence||Overlies Sticht Range Beds.|Volcaniclastic sandstones.|
30392|Back Peak Beds|69876|5|Briefly described|p293|Middle Cambrian|Middle Cambrian|Regional cross-section.||||Underlies Moina Sandstone. Adjacent to Bonds Range Porphyry. Overlies Lorinna Greywacke.||
37231|Badger Head Complex|23990|6|Mentioned|p184|||||||||
860|Badger Head Formation|42877|5|Briefly described|p162|||See also Fig.2, p157. ?Precambrian||||||21-MAR-07
860|Badger Head Formation|65646|6|Mentioned|p55 Fig.29, p57.||Proterozoic|See Badger Head Group. Metasediments.||||||09-JAN-15
860|Badger Head Formation|70025|6|Mentioned|p26|Neoproterozoic|Neoproterozoic|Possible correlative to Burnie Group? Deposited on thinned continental crust?||||||
29232|Badger Head Group|23850|5|Briefly described|p790 Fig. 5|Proterozoic||||||||
29232|Badger Head Group|24216|4|Described|p810|Proterozoic|Proterozoic|Topographically high polydeformed turbidite package. Structurally overlies Port Sorrell Formation.||||||04-JUL-13
29232|Badger Head Group|30887|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29232|Badger Head Group|30889|3|Fully described|p14|||See also p15-20.||||||21-MAR-07
29232|Badger Head Group|31195|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29232|Badger Head Group|33839|5|Briefly described|p567|||||||||
29232|Badger Head Group|37057|6|Mentioned|p505|||||||||
29232|Badger Head Group|38157|6|Mentioned|p286|||||||||
29232|Badger Head Group|60900|5|Briefly described|p887 Fig. 1, p893|||||||||
29232|Badger Head Group|61216|5|Briefly described|p6 Fig. 1|Proterozoic|Proterozoic|Age: pre-777Ma.||||||10-FEB-11
29232|Badger Head Group|61395|3|Fully described|p76-89|Proterozoic|Proterozoic|Age: <777Ma. Resemble rocks of Burnie Formation and Mathinna Gp. See also p1, p26 Fig. 3.1,p91,p94,p96|||||Metasediments/turbidites - well bedded monotonous alternation of quartzwacke and siltstone, and slaty mudstone, moderately well sorted.|02-FEB-16
29232|Badger Head Group|63635|5|Briefly described|p10 Fig. 4|Proterozoic|Proeterozoic|Age: <777Ma. ||||||
29232|Badger Head Group|63675|6|Mentioned|Frontispiece, p5|Neoproterozoic|Neoproterozoic|Quartzwacke turbidite sequence.||||||
29232|Badger Head Group|63890|6|Mentioned|p6, p23|Precambrian|Precambrian|Mentioned in terms of correlation with Precambrian rock types.||||||
29232|Badger Head Group|65646|6|Mentioned|p4 Fig.1.|Proterozoic|Proterozoic|Pre-777 Ma.||||||09-JAN-15
29232|Badger Head Group|66575|5|Briefly described|p934, p935 Fig1, p951 Tb.2,|Cryogenian|Cryogenian|Proterozoic turbidites; detrital zircon max depositional age of ~1070 Ma.||||||
29232|Badger Head Group|67655|6|Mentioned|p5, preface map|Neoproterozoic|Neoproterozoic|Presented as Quartzwacke turbidite sequences (Burnie-Oonah Fm, Badger Head Group and correlates) on map.||||||09-JAN-15
29232|Badger Head Group|69842|6|Mentioned|p8-9|Cambrian|Cambrian|Harford, Port Sorell South and North maps.||||Tentatively correlated with Dundas Group.||
29232|Badger Head Group|69873|5|Briefly described|p53, p66|||Gee and Legge (1979), Reed et al. (2002). Badger Head inlier. Correlative of Oonah Formation and Burnie Group. Three successions long regarded as correlates (e.g. Spry 1962a,1964; Gee 1967a; Turner 1989a; Reed et al. 2002; Black et al. 2004) are Oonah Formation (western Tas; Hills and Carey 1949; Spry 1958a; Brown 1986), Burnie Formation (northern Tas; Spry 1957a), and Badger Head Group (Badger Head Inlier; Gee and Legge 1979; Reed et al. 2002). To simplify nomenclature, we apply the first-used term, Oonah Formation, to all these successions (refer to p53).||||Is faulted against Port Sorell Formation.||21-DEC-15
29232|Badger Head Group|69874|5|Briefly described|p107 Fig 4.9, p110 Fig 4.11, p137|Proterozoic|Proterozoic|See also p138 Fig. 4.37. Along with Burnie Formation, as correlates of Oonah Formation (first-used term), these units are now superseded by Oonah Formation.||||Probable correlate of Oonah Formation.|Turbidite sequence of sandstone, slate and phyllite.|
29232|Badger Head Group|70025|6|Mentioned|p4-5|Tonian|Mesoproterozoic|Sorrell-Badger Head Zone. Abbreviated as BH on p4 Fig 2.|||||Turbidite.|
29232|Badger Head Group|71711|6|Mentioned|p395|||Of Badger Head Inlier. Name superseded, and rocks now included in Oonah Formation.||||||
861|Badger Head Metamorphic Complex|41562|6|Mentioned|p523|||||||||
861|Badger Head Metamorphic Complex|44135|6|Mentioned|p40|||||||||07-DEC-09
861|Badger Head Metamorphic Complex|61411|6|Mentioned|p3. ||Proterozoic|||||||
861|Badger Head Metamorphic Complex|61412|6|Mentioned|p52.||Proterozoic|||||||11-JUN-20
861|Badger Head Metamorphic Complex|66190|6|Mentioned|p469|||||||||
861|Badger Head Metamorphic Complex|69667|6|Mentioned|p960 Fig.1|||Shown as Mesoproterozoic.||||||11-JUN-20
23350|Badger Island granodiorite|36374|3|Fully described|p63|||||||||
40002|Bakes Oil Shale Member|24548|5|Briefly described|p9,12|Permian|Permian|Of the Quamby Mudstone. Max Thickness: 5ft. See also Map 4687.||||||26-MAR-07
24683|Bald Hill complex|36350|6|Mentioned|p3|||||||||
38482|Bald Hill ultramafic complex|23718|6|Mentioned|p55|||Informal name.||||||
78541|Balfour Slates and Sandstones|67502|6|Mentioned|p145|||Replaced by the roughly equivalent Balfour Subgroup, see also Balfour slates and sandstones.||||||
73341|Balfour Subgroup, upper|63250|5|Briefly described|p8, p13|||Informal - see Balfour Subgroup. Porphyroblasts are common in its spotted chloritic siltstone units. ||||||
73348|Balfour slates and sandstones|63167|5|Briefly described|p17|||Originally defined as Interview Slate and Quartzite, now renamed Interview Siltstone. The original definition included Rupert beds. ||||||
73348|Balfour slates and sandstones|67502|6|Mentioned|p24-25.||Neoproterozoic|Replaced by the Balfour Subgroup - defined in this paper (refid 67502). Originally used by Ward (1911), variants have been used by numerous other authors, the unit has not been formally defined previously. See also Balfour Slates and Sandstones in this paper.||||||
73348|Balfour slates and sandstones|69873|6|Mentioned|p43|||Of Ward (1911): obsolete. Approximately equivalent to the Balfour Subgroup (Everard et al., 2007) and to the Interview Siltstone (Gee et al., 1969).||||||
74581|Barnetts Sandstone|63868|2|Defined|p24|Early Triassic||See also Barnetts Member of the Springs Sandstone - names used interchangeably and unclear which takes precedence. Lower part of the Cygnet Coal Measures. Disconformably overlies Cygnet Coal Measures. Thickness: 27m. Feldspathic sandstone.||||||07-FEB-11
73331|Barrington chert|63249|5|Briefly described|p3|||Informal - see Barrington Chert. Mixed siliciclastic and voclaniclastic rocks. ||||||
1245|Bathurst Group""|29875|6|Mentioned|p27|||||||||
1336|Beattie Formation|37412|6|Mentioned|p26|||Name is declared as invalid.||||||
1419|Bell Formation|41695|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
1419|Bell Formation|41795|4|Described|p65|||||||||
1419|Bell Formation|41896|6|Mentioned|p25, p27|||Same as Bell Shale p29||||||
73250|Bell shale|63244|5|Briefly described|p1|Devonian|Devonian|Informal name. Of the Eldon group. Overlies Florence sandstone. Overlain by Bell shale. Richly fossiliferous unit.||||||
1426|Bellingham Formation|22627|6|Mentioned|p132|Ordovician|Ordovician|||||||
1426|Bellingham Formation|23467|5|Briefly described|p290|Silurian|Ordovician|||||||
1426|Bellingham Formation|23850|5|Briefly described|p786|Early Devonian|Ordovician|See also p787 Fig. 2. Of the Panama Group. Overlain by Sidling Sandstone.||||||27-MAR-07
1426|Bellingham Formation|24220|5|Briefly described|p880|Devonian|Cambrian|Of the Panama Group. Originally included in the Mathinna Group. Geological Province: Tabberabberan Orogeny.||||||27-MAR-07
1426|Bellingham Formation|42878|2|Defined|p196|Early Devonian|Early Ordovician|see also Fig.1, p170, p192||||||
1426|Bellingham Formation|44135|5|Briefly described|p41|||Of the Mathinna Group. Thickness: ~2km. Increasingly sand-rich succession of quartzose turbidites of sublithic (~2km) then feldspatholithic composition (Sidling Sandstone, ~2km).||||||07-DEC-09
1426|Bellingham Formation|61216|5|Briefly described|p5, p6 Fig. 1|||Of Mathinna Supergroup. Overlies Turquoise Bluff Slate; underlies Sidling Sandstone.||||||10-FEB-11
1426|Bellingham Formation|61395|5|Briefly described|p3 Fig. 1.2, p20|Pridoli|Pridoli|Of the Mathinna Group. Turbidites. Overlain by Sidling Formation. See also p4 Fig. 1.3.||||||07-FEB-11
1426|Bellingham Formation|63635|5|Briefly described|p9, p23|Late Silurian|Late Silurian|Of the Panama Group (Mathinna Supergroup). Overlies Turquoise Bluff Slate; overlain by Sidling sandstone. Turbidites.||||||
1426|Bellingham Formation|63675|5|Briefly described|p16-17|||Quartzose turbidites of sublithic composition. 2 km thick. Unit in Mathinna Supergroup; overlies Turquoise Bluff Slate; is overlain by Sidling Sandstone.||||||
1426|Bellingham Formation|64396|5|Briefly described|p209 Fig. 1|||Of the Mathinna Group.||||||08-DEC-08
1426|Bellingham Formation|65646|5|Briefly described|p4 Fig.1, p5, p6.|Early Devonian|Late Silurian|Unit in Mathinna Group. Underlies Sidling [misspelt] Sandstone. Separated from underlying Turquoise Bluff Slate by a fault or unconformity.||||||08-FEB-16
1426|Bellingham Formation|67493|5|Briefly described|Figs.1-3, p7-11, p15-6, p19, p62, p72|Early Devonian|Silurian|Unit in Mathinna Group of Powell and Baillie (1992); superseded and placed in Panama Group (Reed 2001). Overlain by Sidling sandstone [sic]. Replaced by three new formations: Lone Star Siltstone, Retreat Formation and Yarrow Creek Mudstone. ||Panama Group|||Turbiditic sandstone-rich sections, quartzose sublitharenite.|
1426|Bellingham Formation|67503|5|Briefly described|p8, p9, p20 |||Thickness ~2km. Replaced by three new Formations: Yarrow Creek Mudstone, Retreat Formation and Lone Star Siltstone. Base of package considered a fault or unconformity, suggested Middle Silurian. Classical turbidite features. Flutes, grooves and other sole marks present but severely modified by strain. Well preserved cross lamination.||||||
1426|Bellingham Formation|67655|4|Described|p17|||Thickness: about 2 km. Deposited in lobes on a submarine fan system.||Mathinna Supergroup||is overlain by Turquoise Bluff Slate (inferred unconformity); overlies Sidling Sandstone|quartzose turbidites of sublithic composition|
1426|Bellingham Formation|69875|4|Described|p264 Fig 5.16, p265-266, p269-270|Ludlow|Wenlock|Powell et al. (1993); in their Mathinna Group, where it overlay their Turquoise Bluff Slate and was overlain by their "Sidling sandstone". Assigned to Panama Group (Mathinna Supergroup) by Reed (2001). Remapping (Seymour et al. 2010) resulted in replacement by 3 lithologically distinct units named Lone Star Siltstone, Retreat Formation and Yarrow Creek Mudstone. ~2km thick. Palaeocurrent patterns indicate lobes on a submarine fan system prograding ENE. Sedimentary environments, facies, provenance and sedimentary structures described.||Panama Group||Overlies Tippogoree Group [Turquoise Bluff Slate]. Underlies "Sidling sandstone".|Classical turbidites of proximal and distal aspect; dominant sandstone composition is quartzose sublitharenite with fissure-type conjugate cleavage.|
1426|Bellingham Formation|69876|5|Briefly described|p276, p278|Early Devonian|Late Silurian|||Panama Group||Overlies Tippogoree Group [Turquoise Bluff Slate] unconformably. Underlies Sidling Sandstone.||
1455|Ben Lomond granite|31577|5|Briefly described|p80|||Slightly less than 370 m.y.||||||
1455|Ben Lomond granite|41471|6|Mentioned|p288|||||||||
1455|Ben Lomond granite|48745|6|Mentioned|p115|||||||||
1455|Ben Lomond granite|64393|6|Mentioned|p80|||||||||07-FEB-11
1481|Benjamin Formation|41954|6|Mentioned|Table 1 P12|||||||||
1482|Benjamin Limestone Lower|41951|5|Briefly described|p94|||||||||
1482|Benjamin Limestone Lower|42107|5|Briefly described|p306|||See also Fig.2||||||
1483|Benjamin Limestone Member|35554|6|Mentioned|p5|||||||||
1484|Benjamin Limestone Upper|41951|5|Briefly described|p94|||||||||
1484|Benjamin Limestone Upper|42107|6|Mentioned|p306|||See also Fig.2.||||||27-MAR-07
1486|Benjamin limestone Lower|41951|6|Mentioned|p94|||||||||
74345|Benson Peak Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
74345|Benson Peak Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
1512|Bernacchian Stage|30150|2|Defined|p97|Early Permian|Early Permian|||||||
1512|Bernacchian Stage|38906|4|Described|p13|||||||||
1512|Bernacchian Stage|38908|6|Mentioned|p6|||||||||
1512|Bernacchian Stage|39680|6|Mentioned|Map legend|Permian|Permian|||||||
73347|Bernafai volcanics|63167|5|Briefly described|p20|||Informal - see Bernafai Volcanics.||||||
26386|Berridale Limestone|29437|6|Mentioned|p154|||||||||
26386|Berridale Limestone|31758|6|Mentioned|Map legend|Permian|Permian|In Cascades Group.||||||
26386|Berridale Limestone|32943|6|Mentioned|p96|||See also P98,105 & 106||||||
26386|Berridale Limestone|38610|6|Mentioned|p307|||||||||
26386|Berridale Limestone|41895|6|Mentioned|p11|||||||||
26386|Berridale Limestone|70096|6|Mentioned|p221|||||||||
26386|Berridale Limestone|70194|6|Mentioned|p299 Fig 2|Artinskian|Artinskian|Incorrectly abbreviated as Berriedale Lat in Fig 2 p299.||||Overlain unconformably by Malbina and Deep Bay formations. Underlain by Nassau Formation. Correlated in part with Cascades Group.||
26386|Berridale Limestone|73327|5|Briefly described|Map legend|Permian|Permian|Map unit also includes Nassau Siltstone and Rayner Sandstone with collective description of dominantly richly fossiliferous, interbedded glaciomarine grey bioclastic and argillaceous limestone and calcareous siltstone; lower beds of fossiliferous siltstone; basal pebbly sandstone bed in northern areas; in part contact metamorphosed by dolerite.||Lower Parmeener Supergroup|||Richly fossiliferous, interbedded glaciomarine grey bioclastic and argillaceous limestone and calcareous siltstone. In part contact metamorphosed by dolerite.|
1521|Berriedale Formation|30150|6|Mentioned|Fig.5|||||||||
1521|Berriedale Formation|36020|6|Mentioned|p388|||||||||
1521|Berriedale Formation|43021|5|Briefly described|Fig.2,p462|||Same as Berriedale Limestone?||||||
1521|Berriedale Formation|67543|6|Mentioned|p145 Fig.4||||||||Limestone.|13-OCT-17
1523|Berriedale limestone|33711|6|Mentioned|p383|||||||||
1523|Berriedale limestone|37477|6|Mentioned|p502|||||||||
1523|Berriedale limestone|38197|6|Mentioned|p684|||||||||
73281|Beulah "granite"|63240|6|Mentioned|p6|||Referred to as Beulah "granite" bodies.  Described as andesite-related intrusive rocks.||||||
24716|Beulah Formation|36788|3|Fully described|p18|||||||||
24716|Beulah Formation|42891|5|Briefly described|Fig.3 p300|||||||||
24716|Beulah Formation|63168|6|Mentioned|p57|||||||||
24716|Beulah Formation|63169|6|Mentioned|p161|||||||||
24716|Beulah Formation|63249|5|Briefly described|p2, p4 Tb. 1|Cambrian|Cambrian|Of Jennings (1959, 1979). Overlies Gog Range Greywacke. Geological Province: Fossey Mountain Trough (Dundas Trough). Andesitic volcanics. ||||||
24716|Beulah Formation|69876|5|Briefly described|p293|Middle Cambrian|Middle Cambrian|Regional cross-section.||||Underlies Gog Range Greywacke, Moina Sandstone. Overlies Lorinna Greywacke, except where Lorinna Greywacke is thrust faulted on top.||
73142|Beulah Formation""|44135|6|Mentioned|p27|||Informal  name of Jennings et al (1959) - for andesitic and basaltic rocks including pyroxene-phyric lava and breccia. Probably superseded by Beulah Granite?||||||07-DEC-09
1558|Beulah Microgranite|36788|5|Briefly described|p37|||||||||
81363|Beulah granite|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Northern Mount Read Volcanics, with U-Pb SHRIMP zircon age of 493.5+\-7.8 Ma.|493.5+\-7.8 Ma.|||||
73332|Beulah granite""|63249|5|Briefly described|p3|Late Cambrian|Cambrian|Informally named monzodiorite - probably of the Beulah Formation. Age: 493.5+/-3.9Ma (zircon U-Pb). ||||||
26391|Billop Formation|24549|4|Described|p8|Permian|Permian|Of the Golden Valley Group. Max Thickness: 20ft. Grey sandstone, containing numerous brachiopod fragments||||||27-MAR-07
26391|Billop Formation|30156|5|Briefly described|p38|||Part of Golden Valley Group.||||||27-MAR-07
26391|Billop Formation|34316|5|Briefly described|p21 Fig.3|Early Permian|Early Permian|Of the Golden Valley Group. Brachiopod conglomerate.||||||06-FEB-08
26391|Billop Formation|36207|6|Mentioned|p27|||||||||
26391|Billop Formation|41699|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
26391|Billop Formation|42000|6|Mentioned|Fig.12 P69|||||||||
26391|Billop Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
26391|Billop Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
75742|Binn's Gully Mudstone|66172|14|Not recorded|23|Permian|Permian|||||||
1710|Birch Inlet Volcanics|41697|6|Mentioned|Map legend|||||||||
37827|Birchs Inlet volcanics|24216|6|Mentioned|p815|||Informal name.||||||
73144|Birchs Inlet-Mainwaring River Volcanics|44135|5|Briefly described|p23, p24|||Informal collective name (Brown et al 1991) for a basaltic volcanic association in two areas: one in Birchs Inlet and the other in a belt trending north from near Veridian Point on west coast.||||||07-DEC-09
73144|Birchs Inlet-Mainwaring River Volcanics|61395|6|Mentioned|p92|||Part of an oceanic fore-arc obducted onto western Tasmania in Early or Middle Cambrian.||||||
1738|Bischoff Formation|41795|6|Mentioned|p19|||||||||
73450|Bischoff Series|63168|6|Mentioned|p50 Tb. 3.1|||Of Reid (1925). ||||||
1739|Bischoff Series""|41795|6|Mentioned|p17|||||||||
30228|Black Harry Beds|43131|3|Fully described|p570|||Should be Black Harry beds.||||||
30228|Black Harry Beds|43164|6|Mentioned|12|||||||||
30228|Black Harry Beds|43777|5|Briefly described|p4|||||||||
30228|Black Harry Beds|63238|5|Briefly described|p19 Fig. 2|Middle Cambrian|Middle Cambrian|Of Mount Charter Group. Overlie Central Volcanic Complex rocks. Discussion of work by previous workers that Mt Charter Group is condensed into the Farrell Slates belt (p21). See also p20 Fig. 3.||||||
30228|Black Harry Beds|64395|5|Briefly described|p172, p174 Fig. 8|||Basal unit in Mount Charter Group (Mount Read Volcanics). Interfinger or overlie Central Volcanic Complex. Rich in mass flow deposits.||||||07-FEB-11
30228|Black Harry Beds|69369|5|Briefly described|p288, p290 Tb.1, p291 Fig.4 |Cambrian|Cambrian|Corbett and Komyshan (1989).||Unit in Animal Creek Greywacke.|||Shard-rich volcaniclastic siltstone with minor volcaniclastic sandstone.|
30228|Black Harry Beds|69874|4|Described|p150, p158, p164-165, p188|||Maximum thickness over 600m. Interfingers with Kershaw Pumice Formation (probably a lateral equivalent).||Mount Charter Group||Underlies Animal Creek Greywacke. Overlies and interfingers with the Northern Central Volcanic Complex. Lateral equivalent of Kershaw Pumice Breccia.|Dominantly vitriclastic mudstone and pumiceous sandstone; local dacitic intrusives and lavas.|
30228|Black Harry Beds|70753|6|Mentioned|p185|||Unfossiliferous.||||||
79475|Black Hill Volcanics|69874|6|Mentioned|p125 Fig 4.23|||Geochemistry diagram. Presumably Cambrian.||||||04-APR-18
73339|Black River Dolomite chert|63250|5|Briefly described|p7, p14|||Informal reference to chert within the more silicified parts of Black River Dolomite. Characteristically a very fissile thinly laminated shale and massive to blotchy or banded chert||||||
1823|Black River Dolomite""|42358|6|Mentioned|p11|||Used 1959. Correlated with the Forest Conglomerate and Quartzite 1968.||||||
1879|Blackwood Conglomerate""|30889|6|Mentioned|p50|||||||||
1881|Blackwood Formation|24549|4|Described|p6|Permian|Permian|Of the Ferntree Group. Max Thickness: 5ft.  An excellent marker formation due to its limited thickness and persistent outcrop||||||27-MAR-07
1881|Blackwood Formation|30156|6|Mentioned|p40|||Part of Bogan Gap Group.||||||27-MAR-07
1881|Blackwood Formation|34316|5|Briefly described|p21 Fig.3|Triassic|Triassic|Topmost unit of the Ferntree Group.||||||06-FEB-08
1881|Blackwood Formation|63172|5|Briefly described|p296 Fig. 8.1, p307|Late Permian|Late Permian|Probably replaced by Blackwood Conglomerate? Of the Bogan Gap Group.||||||07-FEB-11
1881|Blackwood Formation|63263|5|Briefly described|p33 Fig. 7|||Probably misnamed - should be Blackwood Conglomerate?||||||07-FEB-11
31680|Blessingdon Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
2004|Blue Seam|40334|6|Mentioned|Fig.14|||||||||
2004|Blue Seam|63172|5|Briefly described|p337|Late Triassic|Late Triassic|Within the Mount Nicholas Coal Measures at Mt. Nicholas.||||||07-FEB-11
28381|Blue Tier granite|31577|5|Briefly described|p80|||370 m.y.||||||
2011|Bluestone Bay Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Bluestone Bay Granodiorite [M McClenaghan Jan95]||||||
2011|Bluestone Bay Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite; part of South East Coast granites.  I-type granite, mafic; unfractionated, reduced. Name implied from map legend.||||||26-SEP-07
2023|Bluff River Pebbly Siltstone|36817|4|Described|p55|||See also Bluff River Formation p57.||||||
35653|Blyth's Creek Formation|23114|5|Briefly described|p468|||||||||
35653|Blyth's Creek Formation|61395|5|Briefly described|p26 Fig. 3.1, p59|Cambrian|Cambrian|Probably superseded by Blyths Creek Formation - both names used interchangeably in text. Overlain by Salisbury Hill and Eaglehawk Formations.||||||07-FEB-11
35653|Blyth's Creek Formation|65646|6|Mentioned|p55 Fig.29, p57.||Cambrian|Mis-spelt. See Blyths Creek Formation.||||||09-JAN-15
2043|Blyths Creek Formation|30889|6|Mentioned|p23|||||||||
2043|Blyths Creek Formation|61216|5|Briefly described|p6 Fig. 1|Late Cambrian|Late Cambrian|Of Green (1959). Of the Dundas Group.  Includes Dallys Siltstone and Ilfracombe Slate.||||||10-FEB-11
2043|Blyths Creek Formation|61395|3|Fully described|p27 Fig. 3.2, p29, p82-83|Early Paleozoic|Early Paleozoic|Basement stratum in Beaconsfield region (TAS) - now considered to include Blyths Creek Fm and Dally's Siltstone of Green (1959). Inexplicably written as Blyth Creek Formation in p85,p86 Fig 6.5 See also p3 Fig. 1.2, p4 Fig. 1.3.||Of the Dundas Group.||Disconformably underlies the Denison Group. Underlies the Salisbury Hill Formation.|Siliciclastic sedimentary + mafic igneous rocks + minor limestone.|17-DEC-13
2043|Blyths Creek Formation|63251|5|Briefly described|p10 Fig. 3|Cambrian|Cambrian|Of the Dundas Group.||||||
2043|Blyths Creek Formation|64396|5|Briefly described|p210 Fig. 2, p211|Cambrian|Cambrian|Basal unit in the Beaconsfield Goldfield. Consists of layers of white limestone interspersed with conglomerate horizons.||||||16-DEC-13
2043|Blyths Creek Formation|65646|5|Briefly described|p4 Fig.1, p56 Fig.30, p57.||Middle Cambrian|Unit in Dundas Group. Includes Dallys Siltstone and Ilfracombe Slate. Underlies Denison Group. Sequence of shale, limestone, greywacke siltstone, quartz sandstone, and a distinctive conglomerate lower in the sequence. Includes mafic igneous rocks.||||||09-JAN-15
2043|Blyths Creek Formation|69842|5|Briefly described|p8|Cambrian|Cambrian|Beaconsfield, Exeter maps; fossils from this Formation straddle the Tyndall Group-Southwell Subgroup boundary: correlation is uncertain. Tentatively included in undifferentiated Cambrian Sedimentary Sequence.|||||Interbedded shale, greywacke, siliceous to polymict conglomerate, limestone and basaltic andesite.|
2043|Blyths Creek Formation|69874|4|Described|p137, p138 Fig 4.37, p151, p172|Middle Cambrian|Middle Cambrian|Macdonald et al. (2001). Beaconsfield area. May constrain emplacement age of Andersons Creek Ultramafic Complex: contains ultramafic detritus and late Middle Cambrian fossils, in Beaconsfield Mine drill core. Underlies correlates of Tyndall Group siltstones with trilobite rich fauna, tuffaceous siltstones closely associated with andesites at Paradise near Sheffield, Native Track Tier volcaniclastic sandstone sequence. Fossils of late Undillan - early Boomerangian age. ||||Overlies Western Volcano-Sedimentary Sequence. Underlies Tyndall Group correlates.|An interbedded complex of polymict conglomerate, sandstone, siltstone, limestone and slate. Includes locally a lens of altered tholeiitic basalt.|
2043|Blyths Creek Formation|69876|5|Briefly described|p341-342, p344|Cambrian|Cambrian|Informally defined [?] by MacDonald et al. (2001) to include all pre-Denison Group rocks in Beaconsfield district not directly associated with Andersons Creek Ultramafic Complex.||Dundas Group||Unconformably overlies Andersons Creek Ultramafic Complex. Is overlain by Salisbury Hill Formation (Denison Group).|Siltstone with minor interbedded limestone and conglomerate horizons.|
2043|Blyths Creek Formation|70753|5|Briefly described|p188|Middle Cambrian|Middle Cambrian|MacDonald et al. in Reed, (2001). Beaconsfield area. Agnostoid and other species listed.||||Is overlain disconformably by Cabbage Tree Conglomerate.||
2065|Boddys Creek dolerite|36799|4|Described|p12|||||||||
2082|Bogan Saddle Group|33292|6|Mentioned|Fig.18|||||||||
2120|Bold Head Adamellite|37055|5|Briefly described|Fig.1|||||||||
2120|Bold Head Adamellite|44135|5|Briefly described|p6|Early Carboniferous|Early Carboniferous|In eastern part of King Island. Intrusive granitic stock.||||||07-DEC-09
2120|Bold Head Adamellite|64400|6|Mentioned|p8|Late Devonian|Late Devonian|Probably not related to Bold Head Volcanics as ages are a fair distance apart. May have been superseded.||||||07-FEB-11
74596|Bold Head Volcanics|60650|4|Described|p179, p180 Fig. 2|||Of Skipworth Subgroup - upper tholeiites section. Max. thickness: ~300m. Basalt pillows and flows with minor conglomerate and sandstone. See also p181, p185-6. ||||||
74596|Bold Head Volcanics|62516|5|Briefly described|p894|Neoproterozoic III|Neoproterozoic III|Top unit of Grassy Group. Overlies Shower Droplet Volcanics. Age: 579+/-16Ma (Nd-Sm isochron; Meffre et al 2004). Intruded by sills of Grimes Intrusive Suite. Tholeiitic.||||||08-SEP-14
74596|Bold Head Volcanics|63458|6|Mentioned|p897 Fig.19. |Ediacaran|Ediacaran|||Unit in Grassy Group.||||
74596|Bold Head Volcanics|63674|5|Briefly described|p7|Ediacaran|Ediacaran|Of Skipworth Subgroup (Grassy Group). Tholeiitic basalt flows, pillow lavas, and volcaniclastic sandstone and conglomerate. Nd-Sm isochron age of 579 +/- 16 Ma (Meffre et al. 2004).||||||
74596|Bold Head Volcanics|64400|5|Briefly described|p3 Fig. 2|Ediacaran|Ediacaran|Of Skipworth Subgroup (Grassy Gp). Overlies Shower Droplet Volcanics. Porphyritic tholeiitic basalt lavas, interbedded with v. thick mafic volcaniclastic conglomerate containing lava-derived clasts.||||||07-FEB-11
74596|Bold Head Volcanics|68241|6|Mentioned|p27|||Meffre et al., (2004). Replaced by the Grahams Road Volcanics.||||||
74596|Bold Head Volcanics|69841|6|Mentioned|p17-18, p27-|Ediacaran|Ediacaran|Meffre et al. (2004); formerly the "upper tholeiite sequence" of Waldron and Brown (1993). Subsequently named the Grahams Road Volcanics to avoid confusion with the prior Bold Head Granite.||||||
74596|Bold Head Volcanics|69873|6|Mentioned|p76|||Of Meffre et al., (2004). Superseded by Grahams Road Volcanics.||||||
2122|Bold Head adamellite|33218|6|Mentioned|p15|||||||||
2122|Bold Head adamellite|61216|5|Briefly described|p30|||Informal name. Small body in eastern King Island.||||||10-FEB-11
75998|Bold Head granodiorite|65644|5|Briefly described|p6|Devonian|Devonian|May be a faulted sliver of the Grassy granodiorite. Intrudes Proterozoic sediments on King Island.  I-Type. See Bold Head Granodiorite (p22).|||||Porphyritic adamellite-granodiorite, pink K-feldspar phenocrysts.|27-MAR-12
30227|Bonds Range porphyry|43131|6|Mentioned|p569|||Informal name.||||||
30227|Bonds Range porphyry|70274|5|Briefly described|p445,447-448,450,454,460,462|Cambrian|Cambrian|Intrusion within, and contemporaneous with VHMS deposit formation in the Mount Read Volcanics. Also coeval with White Spur Formation and lower part of Mount Charter Group. Crops out along the eastern margin of the MRV over a strike length of 55 km and with a width of up to 3 km. Zircon analysis gives a weighted average 206Pb/238U age of 500.4+\-0.8 Ma. Also contains 1.47 Ga inherited zircon ages, interpreted to be derived from (presumably) underlying Tyennan basement.|500.4+\-0.8 Ma||||Felsic quartz-feldspar+\-biotite porphyry.|
2190|Boobyalla granite|37797|6|Mentioned|p143|||||||||
2358|Bott Conglomerate""|35791|6|Mentioned|p227|||||||||
73639|Boulder Point Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Eddystone Batholith.  I-type granite, mafic to felsic, unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
40414|Bowry granitoids|24604|5|Briefly described|p912|Neoproterozoic|Neoproterozoic|Age: ca 780 Ma. Informal - see the Bowry Formation.||||||
2463|Boyes River Complex|41793|6|Mentioned|p63|||||||||
2463|Boyes River Complex|63168|6|Mentioned|p72|||||||||
2477|Brady formation|29638|4|Described|p28|||Late Triassic||||||
2510|Brassey Hill harzburgites|37056|6|Mentioned|Fig.1|||||||||
28399|Brewery Junction Conglomerate|41814|6|Mentioned|map legend|Cambrian||||||||
73305|Brewery Junction Formation, Lower|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Informal - see Brewery Junction Formation. ||||||
73305|Brewery Junction Formation, Lower|64395|5|Briefly described|p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Informal reference to lower section of Brewery Junction Formation. Of the Dundas Group (lower part).||||||07-FEB-11
73305|Brewery Junction Formation, Lower|69573|6|Mentioned|p659, 661|||||||||
73305|Brewery Junction Formation, Lower|69874|5|Briefly described|p148-149, p163, p168, p215|Mindyallan|Boomerangian|Dundas area. Is of the same age as the Tyndall Group. E. eretes Zone - G. stolidotus Zone. [The text appears equivocal as to its parent unit. It is shown as part of the Lower Dundas Group on p149; is described as being "probably of Tyndall Group age" on p163; and on p168 "the Tyndall Group is considered to be represented by...lower Brewery Junction Formation..."].||||Overlies Razorback Conglomerate. Underlies Upper Brewery Junction Formation and Comet Formation.|Unfossiliferous, siliceous sedimentary sequence. Contains some felsic volcanic detritus.|
73305|Brewery Junction Formation, Lower|70753|6|Mentioned|p183-184|Middle Cambrian|Middle Cambrian|Unfossiliferous.||||Conformably/gradationally overlies Razorback Conglomerate. Is overlain by Upper Brewery Junction Formation (fault contact).||
73307|Brewery Junction Formation, Upper|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Middle Cambrian|Informal - see Brewery Junction Formation.||||||
73307|Brewery Junction Formation, Upper|64395|5|Briefly described|p174 Fig. 8.|Late Cambrian|Middle Cambrian|Informal reference to upper section of Brewery Junction Formation.||||||07-FEB-11
73307|Brewery Junction Formation, Upper|69573|6|Mentioned|p659, 661|||||||||
73307|Brewery Junction Formation, Upper|69874|4|Described|p148, p163, p214-215, p229|Mindyallan|Mindyallan|Brown (1986). Dundas area. E. eretes Zone - G. stolidotus Zone. This, and overlying units of the Dundas Group, are now known to be marine equivalents of the Owen Group.||Dundas Group.||Overlies Lower Brewery Junction Formation. Underlies Comet Formation.|Interbedded turbiditic sandstone, granule conglomerate and siltstone, with a large included (?slide) block of volcaniclastic sandstone. A calcareous zone near the top contains a rich trilobite fauna.|
73307|Brewery Junction Formation, Upper|70753|5|Briefly described|p183-185|Middle Cambrian|Middle Cambrian|Trilobite, agnostoid species listed.||||Overlies Lower Brewery Junction Formation (fault contact).|Includes richly fossiliferous siltstone.|
73271|Brewery Junction Formation, lower|63238|6|Mentioned|p13, p18|Middle Cambrian|Middle Cambrian|Informal - see Brewery Junction Formation.||||||
73271|Brewery Junction Formation, lower|63240|5|Briefly described|p4|||Part of the upper section of the "lower Dundas Group" -  now redesignated as Tyndall Group, based on fossil evidence.||||||
73306|Brewery Junction Formation, upper|63238|6|Mentioned|p13|Late Cambrian|Middle Cambrian|Informal - see Brewery Junction Formation.||||||
2529|Brewery Junction Slate and Tuff|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
2531|Briant Quartzite""|42358|5|Briefly described|p11|||Used 1952.  Now redundant.  Part of Cowrie Siltstone.||||||
29280|Bridport Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Bridport Granodiorite [M.McClenaghan Jan 95].||||||
70301|Bridport granodiorite|61723|6|Mentioned|p817|||Informal name for the northern extension of the Diddleum Granodiorite where it runs beneath thin Cainozoic cover. [non-capitalised 'g' is correct!]||||||
29805|Broken Formation|43054|6|Mentioned|Plate 16|||Referred to in text as broken formation. Apparent informal usage.||||||
2694|Browns Creek Group|42863|5|Briefly described|p12|Late Eocene|Middle Eocene|Clean quartz sandstones.||||||30-JUN-14
2705|Brumby Formation (TAS)|24549|4|Described|p9|Permian|Permian|Of the Golden Valley Group. Max Thickness: 50ft. Highly fossiliferous micaceous mudstone, rich in Fenestella and Stenopora fossils, underlain by limestone containing Spirifers and Eurydesma||||||29-MAR-07
2705|Brumby Formation (TAS)|34316|5|Briefly described|p21 Fig.3|Early Permian|Early Permian|Of the Golden Valley Group. Fossiliferous.||||||06-FEB-08
2705|Brumby Formation (TAS)|38200|6|Mentioned|p74|||||||||
39912|Brumby Formation, Lower|24549|6|Mentioned|p9 (table)|Permian|Permian|Informal - see Brumby Formation||||||
39913|Brumby Formation, Upper|24549|6|Mentioned|p9 (table)|Permian|Permian|Informal - see Brumby Formation||||||
2729|Bryant Hill Quartzite|34701|6|Mentioned|p364|||||||||
2729|Bryant Hill Quartzite|36375|6|Mentioned|p72|||||||||
2729|Bryant Hill Quartzite|67502|6|Mentioned|p43|||Longman and Matthews (1962) suggested this unit was overlain by 'Smithton Dolomite', possibly unconformably.||||||
79478|Bulgobac porphyry|69874|5|Briefly described|p164|||Near Sock Creek, in the Burns Peak to Hellyer mine area. Appears to be one of several large and small shallow syn-volcanic intrusions into a volcano-sedimentary sequence overlying the Northern Central Volcanic Complex.|||||Quartz-feldspar-biotite porphyry.|
2877|Bull Creek Volcanics|30211|5|Briefly described|p17|||||||||
2877|Bull Creek Volcanics|36788|6|Mentioned|p45|||||||||
28412|Bull Rivulet Formation|42425|5|Briefly described|Table 2 p141, p149, p139|||Bouldery till. Derived from the Eldon Range. Age >130,000 years (Henty age), but could be considerably younger.||||||05-SEP-12
28412|Bull Rivulet Formation|69880|5|Briefly described|p517 Table 10.2, 518|Pleistocene|Pleistocene|King Valley. OIS 6. Younger than David Formation.|||||Glacial deposits.|
2982|Bundella Formation|23222|6|Mentioned|Map legend|||||||||
2982|Bundella Formation|30150|6|Mentioned|Fig.5|||||||||
2982|Bundella Formation|30819|6|Mentioned|p107|||||||||
2982|Bundella Formation|31762|6|Mentioned|Map legend|Permian|Permian|||||||
2982|Bundella Formation|31769|6|Mentioned|Map legend|Permian|Permian|||||||
2982|Bundella Formation|31780|6|Mentioned|p12|||||||||
2982|Bundella Formation|32868|6|Mentioned|Fig.17|||||||||
2982|Bundella Formation|36799|4|Described|p17|||||||||
2982|Bundella Formation|41895|6|Mentioned|p11|||FD as Bundella Mudstone P19||||||
2982|Bundella Formation|42000|5|Briefly described|p54|||||||||
2982|Bundella Formation|42144|6|Mentioned|Fig.11 P615|||[Wrong State, should be Tas not NSW. CEBMar95]||||||
2982|Bundella Formation|43021|5|Briefly described|Fig.2,p462|||||||||
2982|Bundella Formation|43022|5|Briefly described|p475|||||||||
2982|Bundella Formation|44135|5|Briefly described|p43, p44|||Of Lower Parmeener Supergroup. Richly fossiliferous siltstone, sandstone and minor limestone.||||||07-DEC-09
2982|Bundella Formation|49644|5|Briefly described|Table|||||||||
2982|Bundella Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Cranky Corner Sandstone, Allandale Formation, lower Pebbley Beach Formation, Callytharra Formation and Golden Valley Group. Geological Province: Tasmanian Basin.||||||
2982|Bundella Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Early Permian|Overlain by Faulkner Group and Nassau Formation and Deep Bay Formation; overlies Woody Island Formation.||||||07-FEB-11
2982|Bundella Formation|63263|5|Briefly described|p34, p45, p61|||Thickness: ~120m. Shallow marine shelf deposit - richly fossiliferous siltstone, with minor sandstone and granule conglomerate; some limestone. See also  p33 Fig. 7.||||||07-FEB-11
2982|Bundella Formation|63592|5|Briefly described|p4 (Abstract), p10 Fig. 4|Triassic|Late Carboniferous|Of the Parmeener Supergroup. Fossiliferous mudstone with sedimentary-hosted gold mineralisation.||||||03-OCT-07
2982|Bundella Formation|65645|5|Briefly described|p19,20,21, 23, p27, 31 appendix|Permian|Permian|Apparently used interchangeably with Bundella Mudstone (p19, p20, Fig 2). Type section on Mount Nassau.||||Overlies Woody Island Siltstone; underlies Deep Bay Formation.|Poorly sorted glaciomarine sandstone, siltstone, mudstone.|30-MAR-12
2982|Bundella Formation|65647|5|Briefly described|Appendix p10, 12|Sakmarian|Asselian|Of lower Parmeener Supergroup, SW of Hobart. 118 m thick. Poorly sorted glacio marine sandstone, siltstone, impure limestone. Loadstones and fossils. Type section at Mount Nassau.Tamarian Stage age. Intruded by Jurassic dolerite.||||||
2982|Bundella Formation|65662|5|Briefly described|p10, p12.|||Type section at Mount Nassau is 118 m thick. Contains a widespread dolerite sheet.||Unit in Lower Parmeener Supergroup.||Overlies Woody Island Siltstone. At Cygnet, is overlain by Deep Bay Formation.|Poorly-sorted glaciomarine sandstone, siltstone and impure limestone; lonestones common; many abundantly fossiliferous beds.|
2982|Bundella Formation|67501|5|Briefly described|p7, p18, Fig.8 p17. |||45 m thick in the Maydena map sheet area.||Parmeener Supergroup (Lower)||Overlies the Woody Island Siltstone, underlies the Faulkner Group and Hickman Formation.|Fossiliferous glaciomarine siltstone, sandstone and minor limestone.|
2982|Bundella Formation|67543|5|Briefly described|p144 Fig 3, p145 Fig.4, p153|Sakmarian|Sakmarian|Contains outsized clasts. Fig.4 suggests correlation with Masseys Creek Group and Kansas Creek beds.||Of the Parmeener Supergroup.||Overlies Woody Island Formation. Is overlain by Liffey Group.|Richly fossiliferous pebbly siltstone, limestone.|
2982|Bundella Formation|69877|5|Briefly described|p364 Fig.7.1, p367-369, p372|Sakmarian|Sakmarian|Fossil species listed.||Unit in Lower Parmeener Supergroup.||Overlies Woody Island Formation. Is interbedded with Darlington Limestone. Correlative with Golden Valley Group. Is overlain by Liffey Group.|Richly fossiliferous siltstone and calcareous siltstone, with sandstone and mudstone; local conglomerate.|
2982|Bundella Formation|69879|6|Mentioned|p454 Fig9.37|Permian|Permian|||||Intruded by Jurassic dolerite, Cygnet Alkaline Complex.||
2982|Bundella Formation|70194|6|Mentioned|p299 Fig 2, p304, p307, p310 Fig10c|Early Permian|Early Permian|Also referred to as Bundella Mudstone p310.||Of Parmeener Supergroup.||Overlain by Nassau Formation and Liffey-Faulkner Groups. Underlain by Quamby Fm and Woody Island Fm.||
2982|Bundella Formation|73321|5|Briefly described|Map legend|Permian|Permian|||Lower Parmeener Supergroup||Overlies the Woody Island Siltstone, underlies the Faulkner Group.|Generally fossiliferous glaciomarine siltstone, calcareous siltstone and sandstone; in part contact metamorphosed by dolerite.|
2982|Bundella Formation|73322|5|Briefly described|Map legend|Permian|Permian|||Lower Parmeener Supergroup||Underlies the Faulkner Group.|Generally fossiliferous glaciomarine siltstone, calcareous siltstone and sandstone, with lonestones; richly fossiliferous central interval with some impure limestone; upper interval dominantly of less fossiliferous micaceous siltstone.|
2982|Bundella Formation|73323|5|Briefly described|Map legend|Permian|Permian|||Lower Parmeener Supergroup||Underlies the Faulkner Group.|Fossiliferous, fissile and non-fissile glaciomarine siltstone and sandstone with lonestones; richly fossiliferous central interval with some impure limestone; upper interval dominantly of less fossiliferous micaceous siltstone. Contact metamorphosed.|
2982|Bundella Formation|73324|6|Mentioned|Map legend|Permian|Permian|Correlate of Bundella Formation is described as sparsely to richly fossiliferous marine siltstone, mudstone, sandstone and impure limestone with lonestones.||||||
2982|Bundella Formation|73327|5|Briefly described|Map legend|Permian|Permian|||Lower Parmeener Supergroup||Underlies the Hickman Formation, Faulkner Group.|Generally fossiliferous glaciomarine siltstone, calcareous siltstone and sandstone; in part contact metamorphosed by dolerite.|
2982|Bundella Formation|73639|6|Mentioned|p3|Permian|Permian|||Lower Parmeener Supergroup||Overlies Woody Island Siltstone. Is overlain by Liffey Group.||
2984|Bundella Mudstone Formation|41895|6|Mentioned|P 22|||||||||
3087|Burnie Formation|12179|5|Briefly described|p971|||Related to earliest stages of extension of a Late Neoproterozoic (c. 600 Ma) rifted margin (Crawford and Berry 1992).||||Intruded by Cooee Dolerite.|Continent-derived turbidites interbedded with pillow basalts.|
3087|Burnie Formation|22627|5|Briefly described|fig3p126, p124|Neoproterozoic|Neoproterozoic|||||||
3087|Burnie Formation|22668|6|Mentioned|p4|||||||||
3087|Burnie Formation|22705|6|Mentioned|Fig.1 p790, p802|||Turbiditic unit.||||||02-JUL-08
3087|Burnie Formation|23191|6|Mentioned|Map Legend|||Correlate of Proterozoic interbedded slaty mudstone and quartzwacke.||||||
3087|Burnie Formation|23326|5|Briefly described|971|Neoproterozoic|Neoproterozoic|Continent-derived turbidite interbedded with minor pillow basalt. Intruded by Cooee Dolerite.||||||21-JUL-13
3087|Burnie Formation|23460|6|Mentioned|p169|||||||||
3087|Burnie Formation|23718|5|Briefly described|p12|Proterozoic|Proterozoic|||||||
3087|Burnie Formation|23923|5|Briefly described|p1216|Precambrian|Precambrian|||||||
3087|Burnie Formation|23932|5|Briefly described|p665 Table 1|Adelaidean|Adelaidean|Age: ~740 Ma.||||||
3087|Burnie Formation|23990|6|Mentioned|p167|||||||||
3087|Burnie Formation|24216|5|Briefly described|p810|||||||||
3087|Burnie Formation|24604|5|Briefly described|p904 Fig. 1, p907|Neoproterozoic|Neoproterozoic|Formation is Fm in text.||||||
3087|Burnie Formation|30197|5|Briefly described|p599|||||||||
3087|Burnie Formation|30889|6|Mentioned|p14|||Proterozoic||||||
3087|Burnie Formation|31174|6|Mentioned|Fig. 38|||Proterzoic||||||
3087|Burnie Formation|33218|6|Mentioned|p5|||||||||
3087|Burnie Formation|33348|5|Briefly described|p135|||Precamb.||||||
3087|Burnie Formation|33839|4|Described|p567|||||||||
3087|Burnie Formation|35153|6|Mentioned|p178|||||||||
3087|Burnie Formation|35288|4|Described|p13|||||||||
3087|Burnie Formation|36046|5|Briefly described|p353|||||||||
3087|Burnie Formation|36337|5|Briefly described|p39|||||||||
3087|Burnie Formation|36534|6|Mentioned|p226|||See also P227.||||||
3087|Burnie Formation|36732|6|Mentioned|p297|||||||||
3087|Burnie Formation|38157|6|Mentioned|p286|||||||||
3087|Burnie Formation|39475|6|Mentioned|p404|||||||||
3087|Burnie Formation|39892|5|Briefly described|p19|||Ages of deformational phase of orogeny.||||||
3087|Burnie Formation|40638|6|Mentioned|p193|||||||||
3087|Burnie Formation|40760|4|Described|p155|||Mention p176 and p191.||||||17-JAN-07
3087|Burnie Formation|40965|6|Mentioned|p146|||||||||
3087|Burnie Formation|41562|6|Mentioned|p527|||||||||
3087|Burnie Formation|41693|6|Mentioned|Map legend|Late Precambrian||||||||
3087|Burnie Formation|42358|6|Mentioned|p59|||||||||
3087|Burnie Formation|42877|6|Mentioned|p162|||||||||
3087|Burnie Formation|42891|5|Briefly described|p298, Fig.3 p300|||||||||
3087|Burnie Formation|43191|6|Mentioned|Fig.3 p42.|||||||||
3087|Burnie Formation|43595|5|Briefly described|p552||Neoproterozoic|||||||
3087|Burnie Formation|44135|4|Described|p7, p25|Mesoproterozoic|Mesoproterozoic|Intruded by Cooee Dolerite. Consists mainly of polydeformed sandy turbidite facies quartzose wacke and slaty mudstone with minor altered mafic pillow lava. Correlates discussed.||||||07-DEC-09
3087|Burnie Formation|50327|5|Briefly described|p300, p302 Fig. 2|Neoproterozoic|Neoproterozoic|Ages: 708+/-6Ma and 711Ma (both K-Ar). Dominated by turbiditic sandstone beds. In NW Tasmania.||||||07-FEB-11
3087|Burnie Formation|60900|5|Briefly described|p885, 888|||The name Oonah Formation has priority and is preferred over Burnie Formation in this paper. Intruded by the Cooee Dolerite.||||||06-JAN-15
3087|Burnie Formation|61216|6|Mentioned|p13, p57|||Turbidites. Correlated with the name Oonah Formation.||||||10-FEB-11
3087|Burnie Formation|61263|6|Mentioned|p463|||In northwest Tasmania.||||||
3087|Burnie Formation|61395|6|Mentioned|p77|Neoproterozoic|Neoproterozoic|Outcropping west of Ulverstone. Resemble rocks of Badger Head Group and Mathinna Group.||||||21-JUL-13
3087|Burnie Formation|61411|5|Briefly described|p6, p10, p16.|Neoproterozoic||Deep water turbidite sequence with interbedded sandstone, siltstone and mudstone. Up to five phases of deformation recognised. Low grade metamorphosed.||||||
3087|Burnie Formation|61412|5|Briefly described|p3, p4 Fig.1, p19.|Neoproterozoic||Deep water turbidite sequence with interbedded sandstone, siltstone and mudstone. Up to five phases of deformation recognised. Low grade metamorphosed. The Oonah Formation is a correlate. Intruded by Cooee Dolerite.||||||16-MAY-17
3087|Burnie Formation|63167|4|Described|p5, p12-13|Precambrian|Precambrian|Thickness: >4500m. Monotonous sequence of greywacke and slaty mudstone with minor altered mafic pillow lava. Occurs near the north coast of Tasmania; its equivalent is Oonah Formation in the west. Intruded by Cooee Dolerite. See also p17-18.||||||
3087|Burnie Formation|63168|6|Mentioned|p80|||Unconformably overlain by basal parts of Beecraft Megabreccia.||||||
3087|Burnie Formation|63169|5|Briefly described|p167||Neoproterozoic|||||||
3087|Burnie Formation|63250|5|Briefly described|p2 Fig. 1|||Quartzwacke turbidite sequence.||||||
3087|Burnie Formation|63612|6|Mentioned|p5|||||||||07-FEB-11
3087|Burnie Formation|63675|6|Mentioned|p5|||Regarded as correlate of Oonah Formation: called Burnie-Oonah Fm in Frontispiece.||||||
3087|Burnie Formation|64393|6|Mentioned|p79|||In Rocky Cape region.||||||07-FEB-11
3087|Burnie Formation|66623|6|Mentioned|p14.|Neoproterozoic|Neoproterozoic|Name replaced by Oonah Formation. Dolerite intrusions that have age and geochemical correlation with Mount Arrowsmith Volcanics.||||Intruded by alkaline dolerites.||
3087|Burnie Formation|67502|6|Mentioned|p16 Fig.1, p24.|Neoproterozoic|Neoproterozoic|Excluded from Rocky Cape Group (Spry, 1957) by Gee (1968).|||||Quartzwacke turbidite sequence.|
3087|Burnie Formation|67655|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Correlated with Oonah Formation. Presented as Quartzwacke turbidite sequences (Burnie-Oonah Fm, Badger Head Group and correlates) on map in preface.||||||09-JAN-15
3087|Burnie Formation|69842|6|Mentioned|p3, 6|||Location of pillow basalts in the Burnie map was taken from Burns. Stowport map; some boundary modifications.|||||Includes pillow basalts.|
3087|Burnie Formation|69857|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Dolomitic mudstone, siltstone and sandstone; includes alkali basalt and dolerite.|
3087|Burnie Formation|69872|6|Mentioned|p24-25 Figs.2.7-2.8, p29|||Rift basin fill. Has been intruded by granites and undergone both W- and E-directed thrusts.||||||
3087|Burnie Formation|69873|5|Briefly described|p35, p37, p39, p53|Proterozoic|Proterozoic|Spry (1957). N Tasmania. A thick quartzwacke turbiditic succession, deformed during Tyennan Orogeny (previously called the Penguin Orogeny). Three successions long regarded as correlates (e.g. Spry 1962a,1964; Gee 1967a; Turner 1989a; Reed et al. 2002; Black et al. 2004) are Oonah Formation (western Tas; Hills and Carey 1949; Spry 1958a; Brown 1986), Burnie Formation (northern Tas; Spry 1957a), and Badger Head Group (Badger Head Inlier; Gee and Legge 1979; Reed et al. 2002). To simplify nomenclature, we apply the first-used term, Oonah Formation, to all these successions (refer to p53).||||Correlative of Oonah Formation. Is overlain locally by Luina Group.||21-DEC-15
3087|Burnie Formation|69874|5|Briefly described|p146, p170-171, p232|Neoproterozoic|Neoproterozoic|Penguin area, north coast. Source of hematite clasts in the Duncan Conglomerate. [Along with Badger Head Group, as correlates of Oonah Formation (first-used term), these units are now superseded by Oonah Formation.]|||||Quartzite; includes zones of hematite (ironstone) mineralisation.|
3087|Burnie Formation|69876|5|Briefly described|p350|Proterozoic|Proterozoic|Skarns located to north of Housetop Granite intrusion.||||Intruded by Housetop Granite.|Dolostones that host base metal-poor magnetite skarns.|
3087|Burnie Formation|70025|4|Described|p4,8,10-11,p13-15,27|Cryogenian|Cryogenian|Burnie Zone. Equivalent to Oonah Formation, and likely derived from Rocky Cape Group. Weakly to moderately deformed. Intrusion of ca. 710 Ma rift tholeiites is coeval with initiation of sedimentation in Beardsmore Group, Tansantarctic Mountains. Minimum age for Burnie Formation is ca. 710 Ma based on K-Ar biotite age from alkaline diorite, thereby interpreted as correlatable to lower Togari Group.|||Includes Goat Island Conglomerate.|Overlain unconformably by Success Creek Group and Crimson Creek Formation..|Deep-water sandstone, mudstone, dolomite and minor mafic rift volcanic rocks.|16-JUL-19
3087|Burnie Formation|70753|5|Briefly described|p183|Neoproterozoic|Neoproterozoic|Northern Tasmania.|||||Quartzwacke sequence.|
3087|Burnie Formation|71711|6|Mentioned|p395|||Of Burnie Inlier. Name superseded, and rocks now included in Oonah Formation.||||||
3087|Burnie Formation|73313|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Included in map unit including Burnie and Oonah Formations and correlates, description of dolomitic mudstone, siltstone and sandstone. Unit of alkali basalt and dolerite is within Burnie and Oonah Formations. Uncertainty indicated between Mesoproterozoic and Neoproterozoic ages.||||||
3087|Burnie Formation|73320|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Dundas, Fossey Mountains and Dial Range Troughs. Map units contain both Burnie and Oonah Formations and correlates; descriptions for map units are quartzwacke turbidite sequences with minor dolomite; quartzwacke of high-grade metamorphic provenance, includes alkali basalt and dolerite. Uncertainty between Mesoproterozoic and Neoproterozoic age indicated.||||Unconformably underlies Success Creek Group and correlates.||
3086|Burnie Formation quartzite|35288|6|Mentioned|p38|||||||||
3089|Burnie Quartzite and Slate|34981|6|Mentioned|p37|||||||||
3089|Burnie Quartzite and Slate|35288|6|Mentioned|p30|||||||||
3090|Burnie Slate and Quartzite|34981|6|Mentioned|Fig. 6|||||||||
3091|Burnie formation|38638|6|Mentioned|p1902|||||||||
3092|Burnie slate and quartzite|35288|6|Mentioned|p70|||||||||
73812|Burnie-Oonah Formation|63169|6|Mentioned|p167, p178|||Not a valid name - refers to the changed name of Burnie Formation now preferred as Oonah Formation - informal compound name for Burnie Formation and Oonah Formation.||||||09-JAN-08
73812|Burnie-Oonah Formation|63675|6|Mentioned|Frontispiece|Neoproterozoic|Neoproterozoic|Quartzwacke turbidite sequences. Burnie Formation regarded as correlate of Oonah Formation.||||||
3257|Cabbage Tree Conglomerate|23114|5|Briefly described|p468|||||||||
3257|Cabbage Tree Conglomerate|30889|6|Mentioned|p23|||||||||
3257|Cabbage Tree Conglomerate|45922|14|Not recorded|p.518,519||Ordovician|Underlain by Ilfracombe Slate. Overlain by Caroline Creek Sandstone and Gordon Limestone.||||||03-APR-07
3257|Cabbage Tree Conglomerate|61395|5|Briefly described|p27 Fig. 3.2, p29, p32|Ordovician|Ordovician|Treated as basal member of Salisbury Hill Fm (Denison Gp) - altho' an appropriate name is not mentioned in this study - (see p4). Max. thickness: 50m (in Beaconsfield Gold Mine area).||Of the Denison Group.||Overlies the Blyths Creek Formation.|In drill core, consists of grey to light brown oligomictic quartz arenite and fine quartz arenite.|13-MAY-16
3257|Cabbage Tree Conglomerate|63168|5|Briefly described|p82|Cambrian|Cambrian|Siliceous conglomerate and sandstone overlying other Cambrian sedimentary rocks in the Beaconsfield area. Overlain by Gordon Group limestone. ||||||
3257|Cabbage Tree Conglomerate|64396|5|Briefly described|p210 Fig. 2, p212 Fig. 3|Ordovician|Ordovician|Probably refers to the basal part only of Cabbage Tree Formation?||||||08-DEC-08
3257|Cabbage Tree Conglomerate|65646|5|Briefly described|p4 Fig.1, p56 Fig.30, p58.|Early Ordovician|Early Ordovician|Basal unit in Salisbury Hill Formation, of the Denison Group.||||||09-JAN-15
3257|Cabbage Tree Conglomerate|67655|6|Mentioned|p17|Middle Devonian|Middle Devonian|in the Beaconsfield area|||||siliciclastic sandstone, siltstone and conglomerate|09-JAN-15
3257|Cabbage Tree Conglomerate|69876|5|Briefly described|p342-345|Ordovician|Ordovician|Lewis (1998). Reassigned by Hills et al. (2001) as the basal unit of Salisbury Hill Formation [and thus needs the rank term Member].||Salisbury Hill Formation||Overlies Dundas Group [Blyths Creek Formation] unconformably.|Quartz pebble conglomerate.|
3257|Cabbage Tree Conglomerate|70753|5|Briefly described|p188|Early Ordovician|Early Ordovician|Beaconsfield area.||||Disconformably overlies Blyths Creek Formation.||
3260|Cabbage Tree Formation|22627|6|Mentioned|p134||Early Ordovician|||||||
3260|Cabbage Tree Formation|23114|5|Briefly described|p468|||||||||
3260|Cabbage Tree Formation|30887|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
3260|Cabbage Tree Formation|30889|3|Fully described|p26|||See also p27.||||||03-APR-07
3260|Cabbage Tree Formation|34701|5|Briefly described|p364|||||||||
3260|Cabbage Tree Formation|35791|6|Mentioned|p228|||||||||
3260|Cabbage Tree Formation|36047|6|Mentioned|p366|||||||||
3260|Cabbage Tree Formation|36380|6|Mentioned|p219|||||||||
3260|Cabbage Tree Formation|37057|6|Mentioned|p506|||||||||
3260|Cabbage Tree Formation|40136|5|Briefly described|p19|||||||||
3260|Cabbage Tree Formation|42877|5|Briefly described|p158|||see also Fig.2, p157.||||||03-APR-07
3260|Cabbage Tree Formation|43668|4|Described|p7||Lancefieldian|||||||
3260|Cabbage Tree Formation|43777|6|Mentioned|p9||Early Ordovician|||||||
3260|Cabbage Tree Formation|44135|5|Briefly described|p28|Early Ordovician|Early Ordovician|Comprises a siliciclastic conglomerate-sandstone sequence.||||||07-DEC-09
3260|Cabbage Tree Formation|63170|5|Briefly described|p193|||Overlain by Flowery Gully Limestone. Rests on Cambrian rocks., probably unconformably. Detailed lithology provided.||||||07-FEB-11
3260|Cabbage Tree Formation|63171|5|Briefly described|p291|Early Ordovician|Early Ordovician|Contains sandstone and quartzite sections in upper parts. Associated with the large gold reef of Beaconsfield.||||||07-MAY-08
3260|Cabbage Tree Formation|63890|6|Mentioned|p8|Ordovician|Ordovician|Mentioned in terms of correlation with Ordovician rock types.||||||
3260|Cabbage Tree Formation|64396|5|Briefly described|p208, p211|Ordovician|Ordovician|Rudite-arenite association of quartzose sandstone + minor conglomerate. Thickness: up to 280m. Grades up into the "Wet Beds" ; also referred to as Cabbage Tree Conglomerate, probably a historical predecessor? Name used interchangeably.||||||
3260|Cabbage Tree Formation|69874|5|Briefly described|p234|Early Ordovician|Early Ordovician|Gee and Legge (1979), Banks and Baillie (1989), for a c.400m thick siliciclastic sequence overlying Middle Cambrian rocks at Beaconsfield. Now divided into Salisbury Hill Formation and the overlying Eaglehawk Gully Formation.||||||
3260|Cabbage Tree Formation|69875|5|Briefly described|p243 Fig 5.2, p249|Early Ordovician|Early Ordovician|Beaconsfield district. Fossil control.||Denison Group||Is overlain conformably by Flowery Gully Limestone. Stratigraphically equivalent to Florentine Valley Formation.||
3260|Cabbage Tree Formation|69880|5|Briefly described|p548|Ordovician|Ordovician|Source of silica, sand and gravel for construction and metallurgy; gravels contain 85% to 99% SiO2. Mined near Beaconsfield.|||||Silica-rich gravels in scree slopes.|
3259|Cabbage Tree Formation(sandstone)|37057|6|Mentioned|p505|||||||||
32588|Cabbage Tree Hill Series|45644|5|Briefly described|Page 1233|||Possibly of Lower Silurian.||||||
3261|Cabbage Tree Hill quartzite|35034|6|Mentioned|p85|||||||||
74196|Cabbage Tree conglomerate|61216|5|Briefly described|p6 Fig. 1|||Informal name - included in Salisbury Hill Formation.||||||10-FEB-11
26445|Cabbagetree Formation|31195|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
40004|Calstock Slate and Subgreywacke|24548|5|Briefly described|Maps 4687 and 4688|Cambrian|Cambrian|Informal - see Calstock Formation.||||||03-APR-07
3395|Cameron Granite|45087|5|Briefly described|p22|||Chem. analyses.||||||
75997|Cap dolostone""|65644|5|Briefly described|p6|Neoproterozoic|Neoproterozoic|10m thick. Correlated with Marinoan glacials on mainland (Nuccaleena Formation).||Of Grassy Group.||Overlies Cottons Breccia.|Pale pink-grey fine grained, laminated dolostone, interbedded with limestone and shale.|27-MAR-12
3490|Cape Grim Beds|32754|6|Mentioned|p71|||||||||
3490|Cape Grim Beds|36119|6|Mentioned|p52|||||||||
3490|Cape Grim Beds|73334|5|Briefly described|Map legend|Neogene|Paleogene|||||Disconformably overlies Slaughter Bluff Volcanic Breccia and Trefoil Island Volcanic Breccia, disconformably underlies Little Trefoil Basalt.|Breccia, conglomerate and fossiliferous calcarenite with Upper Longfordian foraminifera.|
3511|Cape Maurouard Series""|39579|6|Mentioned|p13|||||||||
28432|Cape Portland Appinitic Complex|33354|5|Briefly described|p184|||Anal. Refers Jennings and Sutherland (1969).||||||03-APR-07
3517|Cape Portland Lavas|33354|5|Briefly described|p184|||Anal. Refs. Jennings and Sutherland (1969).||||||03-APR-07
73660|Cape Portland alkaline complex|63592|5|Briefly described|p4 (Abstract)|Cretaceous|Cretaceous|Mineral potential untested. Located in northern Tasmania||||||
3518|Cape Portland complex|33354|6|Mentioned|p180|||Structural relationships||||||
3519|Cape Portland porphyrites and spessartit|33354|5|Briefly described|p180|||Petrology and Chemistry.||||||03-APR-07
3525|Cape Sir John Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Cape Sir John Granodiorite.||||||
3525|Cape Sir John Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Wybalenna Suite. I-type,felsic granite; weakly fractionated, reduced. Name implied from map legend.||||||25-SEP-07
3525|Cape Sir John Granite|71730|6|Mentioned|p33, p35, p37, p58||||||||I-type granite.|
73140|Cape Sorell complex|44135|6|Mentioned|p16|||Informal name. Contains asbestos.||||||07-DEC-09
3526|Cape Sorrell complex|41594|6|Mentioned|p27|||||||||
37276|Cape Wickham Metamorphics|24002|5|Briefly described|p228 Fig.2|Proterozoic|Proterozoic|||||||
37276|Cape Wickham Metamorphics|24098|6|Mentioned|p27 Fig. 2|Proterozoic|Proterozoic|Geological Province: Lachlan Fold Belt (King Island, Tasmania).||||||
74650|Cape Wickham Schist|64400|5|Briefly described|p2 Fig. 1b|Neoproterozoic|Neoproterozoic|Age: 769+/-25Ma.||||||07-FEB-11
69915|Cape Wickham granite|61263|5|Briefly described|p461, p467-468|Neoproterozoic|Neoproterozoic|Informal name. Granite pluton on King Island. Of the Wickham Orogeny.||||||
3579|Carbine Group|30392|6|Mentioned|p593|||||||||
3579|Carbine Group|31172|6|Mentioned|p8|||U. Precambrian. See also P15||||||
3579|Carbine Group|31174|6|Mentioned|p170|||||||||
3579|Carbine Group|32409|6|Mentioned|p581|||||||||
3579|Carbine Group|33839|4|Described|p568|||||||||
3579|Carbine Group|63168|6|Mentioned|p50 Tb. 3.1|||Of Elliston (1951, 1954) and Carey (1953). Name now obsolete - incorporated into the Oonah Formation.||||||
3579|Carbine Group|67502|6|Mentioned|p46|||Gulline (1959).||||||
3578|Carbine Group""|41795|6|Mentioned|p12|||||||||
3653|Caroline Creek Beds|36788|6|Mentioned|p26|||||||||
3653|Caroline Creek Beds|69875|5|Briefly described|p246|||Etheridge (1883), for a fossil locality near Railton. Later, as the Caroline Creek Sandstone, applied to lower Ordovician sandstones throughout W Tasmania (eg Banks, 1962). Here named Caroline Creek Formation to reflect the siltier, more fully marine unit in the Railton-Eugenana area. Best exposed section is in Denny Gorge.||||||
3652|Caroline Creek Beds""|42204|6|Mentioned|p236|||||||||
3655|Caroline Creek Sandstone|13995|5|Briefly described|p82, p101|Middle Ordovician|Early Ordovician|Trilobite species; biogeographic links discussed.||||Lateral equivalent of Cashions Creek Limestone.||
3655|Caroline Creek Sandstone|24548|3|Fully described|p6|Ordovician|Ordovician|Parent: Junee Group. Overlying Unit: Gordon Limestone (conformable). Underlying Unit: Owen Conglomerate (conformable). Max Thickness: ~1000ft. Formerly the Caroline Creek beds. Fossiliferous with cephalopods, gastropods and Tritoechia careyi Brown.||||||
3655|Caroline Creek Sandstone|29875|6|Mentioned|p21|||||||||
3655|Caroline Creek Sandstone|30277|6|Mentioned|p212|||Refers Banks(1962) on P147||||||
3655|Caroline Creek Sandstone|30279|6|Mentioned|p122|||Part of Junee Group, Banks (1962).||||||
3655|Caroline Creek Sandstone|30889|6|Mentioned|p23|||||||||
3655|Caroline Creek Sandstone|31461|6|Mentioned|p47|||||||||
3655|Caroline Creek Sandstone|31464|6|Mentioned|p375|||Refers Banks (1962)||||||
3655|Caroline Creek Sandstone|31572|6|Mentioned|p23|||Ordovician||||||
3655|Caroline Creek Sandstone|33731|6|Mentioned|p614|||Trilobites.||||||
3655|Caroline Creek Sandstone|35118|6|Mentioned|p429|||||||||
3655|Caroline Creek Sandstone|36047|5|Briefly described|p365|||||||||
3655|Caroline Creek Sandstone|36788|6|Mentioned|p25|||||||||
3655|Caroline Creek Sandstone|36957|6|Mentioned|p142|||||||||
3655|Caroline Creek Sandstone|40127|6|Mentioned|p11|||||||||
3655|Caroline Creek Sandstone|40136|5|Briefly described|p20|||||||||
3655|Caroline Creek Sandstone|42354|6|Mentioned|p10|||||||||
3655|Caroline Creek Sandstone|42478|4|Described|p10|||Also p12.||||||01-MAY-08
3655|Caroline Creek Sandstone|43668|6|Mentioned|p8|Yapeenian|Bendigonian|||||||
3655|Caroline Creek Sandstone|45118|6|Mentioned|p3|||||||||
3655|Caroline Creek Sandstone|45922|14|Not recorded|p.518,519|||||||||
3655|Caroline Creek Sandstone|48846|14|Not recorded|p15,17,23,24,25|||||||||
3655|Caroline Creek Sandstone|62794|6|Mentioned|p299|Early Ordovician|Early Ordovician|Northern Tasmania. Contains trilobites and brachiopods suggesting uppermost levels may be coeval with Horn Valley Siltstone, Amadeus Basin NT, but faunas have little in common.||||||
3655|Caroline Creek Sandstone|63170|5|Briefly described|p188, p192|Arenig|Arenig|Sandstone unit in the Denison Group which is part of a sandstone-siltstone sequence containing trace fossils (burrows) and body fossils, species of brachiopods, gastropods, a bivalve, cephalopods and trilobites.||||||07-FEB-11
3655|Caroline Creek Sandstone|63890|6|Mentioned|p8|Ordovician|Ordovician|Mentioned in terms of correlation with Ordovician rock types.||||||
3655|Caroline Creek Sandstone|69874|6|Mentioned|p214, p239|Middle Ordovician|Early Ordovician|Correlated with an un-named sedimentary sequence at the Davey River.||||||
3655|Caroline Creek Sandstone|69875|5|Briefly described|p246|||Originally the Caroline Creek Beds of Etheridge (1883), for a fossil locality near Railton. Later, as the Caroline Creek Sandstone, applied to lower Ordovician sandstones throughout W Tasmania (eg Banks, 1962). Here named Caroline Creek Formation to reflect the siltier, more fully marine unit in the Railton-Eugenana area. Best exposed section is in Denny Gorge.||||||
3655|Caroline Creek Sandstone|70025|6|Mentioned|p4|Middle Ordovician|Late Ordovician|Burnie Zone. Abbreviated as CS on p4 Fig 2.|||||Shallow water sandstone.|
3655|Caroline Creek Sandstone|71284|5|Briefly described|p492|||Northern Tasmania. The subject of unverified reports of Iapetognathus conodonts.||||||
3654|Caroline Creek Sandstone""|30277|6|Mentioned|p217|||Refers Banks(1962)||||||
3654|Caroline Creek Sandstone""|32783|6|Mentioned|p1037|||||||||
3656|Caroline Creek Sandstones and Shales|30277|6|Mentioned|p212|||Refers Hills and Carey 1949.||||||
40005|Caroline Creek beds|24548|6|Mentioned|p6|Ordovician|Ordovician|Superseded by Caroline Creek Sandstone||||||
3736|Cashion Creek Limestone|41694|6|Mentioned|Map legend|Ordovician||||||||
3736|Cashion Creek Limestone|42416|6|Mentioned|p191|||||||||
3737|Cashions Creek Formation|36047|6|Mentioned|Table 3|||||||||
3737|Cashions Creek Formation|36957|6|Mentioned|p142|||||||||
3737|Cashions Creek Formation|38211|6|Mentioned|p193|||||||||
3737|Cashions Creek Formation|41317|5|Briefly described|p174|||||||||
3737|Cashions Creek Formation|41854|6|Mentioned|p103|||||||||
3737|Cashions Creek Formation|41954|6|Mentioned|Table 1 P12|||||||||
3737|Cashions Creek Formation|50091|5|Briefly described|p409 Fig. 2, p413 Tb. 1|Ordovician|Ordovician|Of the Gordon Subgroup.  Conodonts found in Florentine Valley.  Name used interchangeably with Cashions Creek Limestone in article.||||||03-APR-07
3739|Cashions Creek limestone|41793|6|Mentioned|p56|||||||||
3749|Casterton beds|13516|6|Mentioned|p174|||Otway Basin||||||
3749|Casterton beds|22944|6|Mentioned|p5.3||Jurassic|||||||
3749|Casterton beds|42318|6|Mentioned|Fig.5 P12|||Variation of old Casterton Beds?||||||
3749|Casterton beds|42361|3|Fully described|p4|Late Jurassic||||||||
3749|Casterton beds|42545|5|Briefly described|Fig.4 P15|||||||||
3749|Casterton beds|42599|5|Briefly described|Fig.3 P614|||||||||
3749|Casterton beds|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
3749|Casterton beds|43052|5|Briefly described|Table 2.1|||||||||
3749|Casterton beds|43747|5|Briefly described|p5||Late Jurassic|||||||
3749|Casterton beds|63173|5|Briefly described|p341|Late Jurassic|Late Jurassic|Geological Province: Otway Basin.||||||07-FEB-11
74918|Castle Carey Formation|64393|5|Briefly described|p80|||An upper glaciomarine sequence within the Parmeener Supergroup.||||||07-FEB-11
3781|Cateena Group""|35791|5|Briefly described|p227|||Refs Burns(1964). 1 of 5 major strat.units in Cambrian Dial Range Trough||||||
3783|Cateena Mudstone|42891|5|Briefly described|Fig.3 P300|||||||||
3783|Cateena Mudstone|42972|6|Mentioned|p172|||||||||
3783|Cateena Mudstone|61411|6|Mentioned|p7.||Middle Cambrian|Overlies Isadulla Conglomerate. Intercalated with Kerrison Volcanics.||||||
24831|Cato Creek microgranodiorite|39927|6|Mentioned|p305|||Misspelling of Catos Creek Microgranodiorite? [Comment added 4-AUG-94]||||||
3794|Cato's Creek Granite|42726|5|Briefly described|map legend|Middle Devonian||Misspelling/variation of Catos Creek Microgranodiorite.||||||
78559|Catos Creek Dyke|67503|4|Described|p9-13 and throughout.|Givetian|Givetian|Associated (geochemical and mineralogical = comagmatic) with St Marys Porphyrite. Intruded along major faults, post-dates major tectonic structures of country rocks. Outcrop displaced by Orieco Fault, to south = largely hornblende-granodiorite, to north = granodiorite, quartz porphyry, adamellite composite.|388 +/- 1 Ma Rb-Sr and K-Ar (Turner et al. 1986).|||Intrudes the sediments of the Mathinna Supergroup. Feeder to the St Marys Porphyrite. Related to the Scamander Tier Dyke.|Hornblende granodiorite, granodiorite, quartz porphyry and adamellite.|27-MAY-14
73643|Catos Creek Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Scamander Tier Suite,  Blue Tier Batholith. I-type granite, mafic; unfractionated, reduced. Name implied from map legend.||||||
73643|Catos Creek Granite|69876|6|Mentioned|p306 Tb 6.1|||||Scamander Tier Suite|||I-type.|
3802|Catos Creek Microgranodiorite|40310|6|Mentioned|p248|||Mention p249 and Fig.5 as C. C. microgranodiorite||||||03-APR-07
28444|Catos Creek granodiorite|40310|6|Mentioned|p249|||||||||
3803|Catos Creek microgranodiorite|40310|6|Mentioned|p249|||See Fig.5||||||
3803|Catos Creek microgranodiorite|40660|6|Mentioned|Fig.10|||||||||
79481|Caudreys Hill Orthopyroxenite|69874|4|Described|p111 Fig 4.12, p123 Fig 4.21|Middle Cambrian|Early Cambrian|See also p125 Fig 4.23, p129. Also appears as Caudreys Hill Pyroxenite and Caudrys Hill Pyroxenite (both on p129) and Caudreys Hill orthopyroxenite member. Western Cumulate of Heazlewood River Complex.||Caudreys Hill Pyroxenite||Lower member of Caudreys Hill Pyroxenite.|Orthopyroxenite; massive, coarse grained (3-20mm) adcumulate olivine orthopyroxenite, with minor interlayers (1-5m thick) of serpentinised dunite and harzburgite.|
3817|Caudreys Hill pyroxenites|37056|6|Mentioned|Fig.1|||||||||
3867|Central Plateau Till|30524|6|Mentioned|Table 2|||Lithostratigraphical relationships. Pleistocene||||||
74642|Central Plateau Volcanics|42244|5|Briefly described|p51|||Not intended as a formal name - general compound term for volcanic rocks of the central plateau region of Tasmania.  The rocks are mainly flow remnants in the region of lakes Sorell and Crescent.||||||12-AUG-08
73141|Central Volcanic Complex""|44135|5|Briefly described|p16|||Informal name for an association in Mt Read Volcanics. Relatively proximal volcanic sequence rich in submarine lavas and pumice breccias which interfingers with the western sequences and contains a number of major polymetallic orebodies.||||||07-DEC-09
3869|Central Volcanics|41562|5|Briefly described|p530|||||||||
40507|Central Volcanics Complex|23947|6|Mentioned|p1074 Fig.1|||Misspelt - see Central Volcanic Complex.||||||03-APR-07
3894|Chamberlain Shale""|40890|6|Mentioned|p54|||||||||
4058|Chudleigh Limestone|40127|6|Mentioned|p10|||||||||
4058|Chudleigh Limestone|40136|5|Briefly described|p27|||||||||
4058|Chudleigh Limestone|42478|5|Briefly described|p15|||Superseded by Chudleigh Subgroup.||||||
4057|Chudleigh Limestone Subgroup|41954|5|Briefly described|p11|Ashgill|Whiterockian|Probable misspelling of Chudleigh Group.||||||
4057|Chudleigh Limestone Subgroup|69875|6|Mentioned|p256|||Mole Creek. See also references to Chudleigh Subgroup (p253, p256).||||||
4065|Churchill Sandstone|40136|6|Mentioned|p24|||||||||
4065|Churchill Sandstone|41793|6|Mentioned|54|||||||||
4106|Clarke Island granite|36374|3|Fully described|p57|||||||||
4109|Clarke Series|33630|6|Mentioned|p908|||||||||
4114|Claun Formation|33494|6|Mentioned|p45|||Misspelling of Cluan on table||||||
4129|Clear-Creek Formation|42227|6|Mentioned|p32|||Incorrect format for name - see Clear Creek Formation.||||||16-JUN-09
4130|Clearwater Bay Sandstone|33732|4|Described|p108|||Base unit of Spero Bay Group.||||||
4130|Clearwater Bay Sandstone|41317|6|Mentioned|p172|||Probable correlate of Denison Group (Late Cambrian to Middle Ordovician)||||||
4130|Clearwater Bay Sandstone|43547|14|Not recorded|Tb p152,p158-60||Emsian|Part of Spero Bay Group||||||
4131|Clearwater Bay lamprophyres|33354|5|Briefly described|p183|||Petrology.||||||
37232|Cleveland Waratah complex|23990|6|Mentioned|p168 Fig.1|||||||||
73274|Cleveland-Waratah Association|63238|5|Briefly described|p11, p22|||Informal name for an allochthonous suite.||||||
73274|Cleveland-Waratah Association|63240|5|Briefly described|p4|||Mafic greywacke sequence.||||||
73274|Cleveland-Waratah Association|63612|5|Briefly described|p13|||||||||07-FEB-11
78476|Cleveland-Waratah Formation|67501|6|Mentioned|p11|Cambrian|Cambrian||||||Basalts.|
78587|Cleveland-Waratah association|63675|6|Mentioned|p7|Cambrian|Cambrian|Contains lithicwacke, red mudstone, chert, mafic volcanics, and rare carbonate rocks that host Devonian skarn mineralisation (Cleveland mine).||||||
78587|Cleveland-Waratah association|69842|6|Mentioned|p5, 7-10|||Montana map; possible outcrop of a correlate in the Golden Valley area. Ulverstone map; a small area of this unit E of Goat Island is potentially Togari Group: needs field checking. Luina map; minor modification to codes and colours, also minor correction to the geology in the Godkin Ridge-Crescent Spur area. Trial map; now includes Cambrian rocks in the Little Henty River-Avebury area.||||Correlated with Ragged Basin Complex.||
78587|Cleveland-Waratah association|69873|5|Briefly described|p35, p68|Early Cambrian|Early Cambrian|Of Williams (1989); later Luina Group.|||||Allochthonous, unfossiliferous sandstone-basalt-chert-mudstone-sandstone sequence.|
78587|Cleveland-Waratah association|69874|5|Briefly described|p110|Early Cambrian|Early Cambrian|Williams (1989). Luina-Waratah area. Renamed in this article as the Luina Group.|||||An unfossiliferous succession of feldspathic and lithicwacke sandstone, chert, mudstone and basalt.|
4169|Climie Formation slate|39892|6|Mentioned|p32|||||||||
4171|Climie Slate and Tuff|31572|6|Mentioned|Fig.|||Upper Cambrian. Correlation chart 1.||||||04-APR-07
4171|Climie Slate and Tuff|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
4171|Climie Slate and Tuff|41795|6|Mentioned|p44|||||||||
4176|Clog Tom Sandstone Formation|30819|6|Mentioned|p108|||||||||
4190|Cluan Sandstone|35280|6|Mentioned|p148|||||||||
4190|Cluan Sandstone|45042|6|Mentioned|p13|||Triassic. See also pp31,33,34.||||||04-APR-07
39914|Cluan formation|24549|6|Mentioned|p3, 5|||Informal - see Cluan Formation.||||||04-APR-07
31305|Coast Range Granite|43547|14|Not recorded|no card|||no card||||||
79484|Colebrook Hill Ultramafic Complex|69874|5|Briefly described|p119 Table 4.2, p131-132|||Brown (1986). Appears as Colebrook Hill UC. A fault-bounded, sheared serpentinite body up to 300m wide. A probable extension under glacial outwash of Huskisson River Ultramafic Complex [and therefore is redundant?].|||||Contains irregular pods and blocks of layered pyroxenite and dunite succession cumulates.|
73814|Colebrook Hill complex|63169|5|Briefly described|p158|||Informal reference to an ultramafic rock association (layered pyroxenite-dunite succession) at Colebrook Hill. Geological Province: Dundas Trough.||||||31-OCT-07
33473|Coles Bay Adamellite|44105|5|Briefly described|p258,259|||Age: mid-Palaeozoic||||||
4324|Coles Bay Granodiorite|37797|6|Mentioned|Table 2|||||||||
4325|Coles Bay granite|37797|6|Mentioned|p144|||||||||
4325|Coles Bay granite|41777|6|Mentioned|Fig.2|||||||||
4326|Coles Bay granodiorite|37797|6|Mentioned|p139|||||||||
24862|Comet Formation|31464|6|Mentioned|Fig.2|||Correlation chart||||||
24862|Comet Formation|35155|6|Mentioned|Table.1|||Reference Blissett (1962).||||||
24862|Comet Formation|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tas. See also p224.||||||04-APR-07
24862|Comet Formation|41795|6|Mentioned|Fig.13|Late Cambrian||||||||
24862|Comet Formation|42608|6|Mentioned|p59|||Mentioned as Fernflow-Comet-Fernfield-Climie Formations||||||
24862|Comet Formation|43777|6|Mentioned|Fig. 2 (at end)||Late Cambrian|||||||
24862|Comet Formation|63168|5|Briefly described|p75 Fig. 3.10, p77|||Of Jago (1979). Superseded by Comet Slate. ||||||
24862|Comet Formation|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Late Cambrian|Of "Upper Dundas Group".||||||
24862|Comet Formation|69874|5|Briefly described|p149, p229|Idamean|Idamean|Dundas area. A 250m thick unit. Now known to be a marine equivalent of the Owen Group [p163].||Dundas Group||Overlies Upper Brewery Junction Formation.|Siltstone and mudstone.|
24862|Comet Formation|70753|6|Mentioned|p184|Late Cambrian|Late Cambrian|See also Comet Slate (p185).||||||
4390|Comet Slate and Tuff|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
4391|Comet Slate""|35791|6|Mentioned|p226|||||||||
4391|Comet Slate""|41795|6|Mentioned|p44|||||||||
73308|Comstock Chert|63238|6|Mentioned|p8|||Presented as Comstock Chert body. ||||||
73308|Comstock Chert|64395|6|Mentioned|p175|||Name is probably informal? Chert sinter exhalite deposit.||||||07-FEB-11
73308|Comstock Chert|69874|5|Briefly described|p201, p203|||A very large mass, 100m thick and over 300m wide, of hard pale cherty silica replacement. Locally highly brecciated; significant Cu-rich polymetallic mineralisation, and weakly mineralised in gold and base metals.||||||
81364|Comstock Formation, lower|70274|5|Briefly described|p460|Cambrian|Cambrian|[Is this the same unit as Comstock Tuff?] Contains an allochthonous block 30m x 30m x 5m of welded rhyolitic ignimbrite hosted in submarine crystal-rich volcaniclastic facies (White and McPhie, 1996, 1997), with a weighted average 206Pb/238U age of 496.0+\-0.9 Ma.||Unit of Tyndall Group.||||
4409|Comstock Tuff|638|5|Briefly described|p104, p105|||Of Corbett et al (1974). Of the Tyndall Group. Overlain by "Jukes Conglomerate". Comprises quartz-feldspar-phyric crystal-lithic tuff, breccia, agglomerate, shale and sandstone. ||||||
4409|Comstock Tuff|23402|5|Briefly described|p18|Late Cambrian|Late Cambrian|Of the Tyndall Group.   Age: 494+/-8Ma (Ar-Ar and SHRIMP).||||||04-APR-07
4409|Comstock Tuff|23718|5|Briefly described|p45|||Of Tyndall Group.||||||
4409|Comstock Tuff|30276|6|Mentioned|p16|||||||||
4409|Comstock Tuff|30278|3|Fully described|p180|||Late Mesial or early Late Cambrian(Jago et al.,1972)||||||
4409|Comstock Tuff|32794|5|Briefly described|p606|||||||||
4409|Comstock Tuff|33218|6|Mentioned|p11|||||||||
4409|Comstock Tuff|35118|6|Mentioned|p428|||||||||
4409|Comstock Tuff|35791|6|Mentioned|Fig.2|||Middle & Late Cambrian correlation chart for Tas.||||||
4409|Comstock Tuff|35844|6|Mentioned|p11|||Stratigraphy. See also p24,37,38.||||||24-MAY-07
4409|Comstock Tuff|36054|6|Mentioned|p437|||||||||
4409|Comstock Tuff|36161|6|Mentioned|Fig.1|||||||||
4409|Comstock Tuff|36817|6|Mentioned|p122|||||||||
4409|Comstock Tuff|37045|6|Mentioned|p213|||||||||
4409|Comstock Tuff|37046|6|Mentioned|p231|||||||||
4409|Comstock Tuff|37047|6|Mentioned|Fig.1|||||||||
4409|Comstock Tuff|39892|6|Mentioned|p28|||||||||
4409|Comstock Tuff|40070|4|Described|p12|||||||||
4409|Comstock Tuff|41148|6|Mentioned|p1245|||||||||
4409|Comstock Tuff|41695|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
4409|Comstock Tuff|41795|6|Mentioned|p53|||||||||
4409|Comstock Tuff|42976|5|Briefly described|p267|||||||||
4409|Comstock Tuff|43054|5|Briefly described|p9|||of Tyndall Group||||||
4409|Comstock Tuff|43131|5|Briefly described|p569|||||||||
4409|Comstock Tuff|43133|6|Mentioned|p613|||||||||
4409|Comstock Tuff|43164|6|Mentioned|22||Cambrian|||||||
4409|Comstock Tuff|43245|6|Mentioned|Map Legend||Cambrian|||||||
4409|Comstock Tuff|43777|6|Mentioned|p3|Late Cambrian|Middle Cambrian|||||||
4409|Comstock Tuff|43781|6|Mentioned|p4||Boomerangian|U/Pb age: 494+/-3.8 Ma. (Middle Boomerangian)||||||
4409|Comstock Tuff|63170|5|Briefly described|p189|||Volcanic and partly-marine sequence.||||||07-FEB-11
4409|Comstock Tuff|64395|5|Briefly described|p171 Fig. 3, p174 Fig. 8|Middle Cambrian|Middle Cambrian|||||||07-FEB-11
4409|Comstock Tuff|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Tyndall Group, with U-Pb SHRIMP zircon age of 439.9+\-2.8 Ma.|439.9+\-2.8 Ma|||||
33866|Comstock Tuff""|22551|6|Mentioned|p149|||||||||
40511|Comstock chert|23948|6|Mentioned|p1089|||Informal name.||||||04-APR-07
4412|Concert Schist quartzite|35670|6|Mentioned|p20|||||||||
24863|Concert Schist""|41795|6|Mentioned|p17|||||||||
4455|Constable Creek Granite|35826|3|Fully described|p130|||||||||
4455|Constable Creek Granite|71730|6|Mentioned|p35, p42, p47, p56|||Highest heat generation of the Scottsdale Batholith, described as a fine-grained marginal phase of the Mt Pearson Granite.|||||I-type granite.|
4456|Constable Creek granites and adamellites|35827|5|Briefly described|p38|||||||||
4479|Cooee Dolerites|32766|6|Mentioned|p272|||||||||
4480|Cooee Dolorite|23326|6|Mentioned|972|||Dykes and synsedimentary sills.||||||18-APR-07
4480|Cooee Dolorite|33218|6|Mentioned|p5|||||||||
4482|Cooee Point Dolerite|37501|6|Mentioned|p407|||Variation of Cooee Dolerite?||||||
4483|Cooee dolerite|30197|6|Mentioned|p601|||||||||
35384|Coralline Member""|23187|6|Mentioned|p245,254|||||||||
4732|Corinna Slates|38638|6|Mentioned|Fig.2|||||||||
4732|Corinna Slates|39475|6|Mentioned|Fig.1|||||||||
24878|Corn Hill Beds|42877|5|Briefly described|Fig.2 p157|||||||||18-SEP-07
24878|Corn Hill Beds|61216|5|Briefly described|p6 Fig. 1|Pridoli|Pridoli|Of Mathinna Group.||||||10-FEB-11
24878|Corn Hill Beds|61395|4|Described|p34, p27 Fig. 3.2|Early Devonian|Late Ordovician|Max. thickness (truncated): 1000m. See also p4 Fig. 1.3, p26 Fig. 3.1.||Of the Mathinna Group.||Overlies Flowery Gully Limestone.|Consists largely of foliated micaceous shaley siltstones with lesser quartzwacke sandstones.|17-JUL-15
24878|Corn Hill Beds|63635|5|Briefly described|p10 Fig. 4|Early Devonian|Ashgillian|||||||
24878|Corn Hill Beds|65646|6|Mentioned|p4 Fig.1, p55 Fig.29, p61 Fig.31.|Devonian|Silurian|Probably an alternative (?earlier) name for Corn Hill Formation.||||||09-JAN-15
42330|Cornubian granites|24273|6|Mentioned|p1667|||||||||
4742|Corra Lynn basalt|33344|4|Described|p50|||Tertiary. Petrology.||||||
78777|Cotton Tree Breccia|63458|6|Mentioned|p900.|||NW Tasmania.|582 Ma (minimum).||||Includes a carbonate unit with characteristics consistent with 'cap carbonates'.|
4782|Cottons Creek Breccia|33218|6|Mentioned|p13|||Variation of 'Cottons Breccia'?||||||
73876|Counsel Creek limestones|24552|5|Briefly described|p8|||Informal. See Counsel Creek Formation.||||||07-FEB-11
78546|Cowrie Formation|67502|6|Mentioned|p29|||Misspelling of Cowrie Siltstone, referred to elsewhere in this paper.||||||
4815|Cox Bight tin granite|35300|6|Mentioned|p1053|||||||||
4821|Coxs Bight tin granite|31525|6|Mentioned|p1053|||Misspelling of Cox Bight ?||||||
4833|Cradle Cirque Formation|23837|6|Mentioned|p440 Fig.2|||||||||
4833|Cradle Cirque Formation|30155|6|Mentioned|Fig.33.4|||||||||
4833|Cradle Cirque Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
4833|Cradle Cirque Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
4851|Crassatella Beds""|41398|6|Mentioned|p1|||||||||
28482|Crassatella bed""|30877|6|Mentioned|p29|||Now Freestone Cove Sandstone||||||
40351|Creemson Creek Formation|23923|5|Briefly described|p1216|Cambrian|Cambrian|||||||
4880|Crescent Spur Group|30293|6|Mentioned|p629|||||||||
4880|Crescent Spur Group|30294|6|Mentioned|p864|||Cambrian ?||||||
4881|Crescent Spur Mica Sandstone Formation|30293|6|Mentioned|p629|||||||||
4881|Crescent Spur Mica Sandstone Formation|30294|5|Briefly described|p864|||See also Fig.5.||||||
73440|Crescent Spur Sandstone""|63168|6|Mentioned|p57|||Of Cox and Glasson (1971) and Collins (1983). Informal name. In Cleveland-Waratah area.||||||
4883|Crescent Spur mica sandstone|33218|5|Briefly described|p27|||||||||
4884|Cresent Spur Group|31435|6|Mentioned|p49|||||||||
4894|Crimson Creek Argillite|30278|5|Briefly described|p173|||See also p186.||||||17-JAN-07
4894|Crimson Creek Argillite|30281|6|Mentioned|p7|||Refers Taylor(1954)||||||
4894|Crimson Creek Argillite|33218|6|Mentioned|Fig.19|||||||||
4894|Crimson Creek Argillite|33839|4|Described|p569|||||||||
4894|Crimson Creek Argillite|33853|6|Mentioned|Fig.1|||Camb.||||||
4894|Crimson Creek Argillite|35092|6|Mentioned|p108|||||||||
4894|Crimson Creek Argillite|40736|6|Mentioned|Fig.1|||||||||
73441|Crimson Creek Argillite""|63168|5|Briefly described|p54|||Defined by Taylor (1954) as dominantly compact mudstone with volcaniclastic and lava horizons. Superseded by Crimson Creek Formation. ||||||
4895|Crimson Creek Argillites|32409|5|Briefly described|p582|||||||||
40342|Crimson Creek Basalts|23932|6|Mentioned|p675|||Geological Province: Dundas Trough.||||||
4896|Crimson Creek Beds|34502|6|Mentioned|Fig.1|||Cambrian||||||
73340|Crimson Creek Formation basalts|63250|6|Mentioned|p5|||Informal - see Crimson Creek Formation. ||||||
4897|Crimson Creek Formation beds|36817|6|Mentioned|p30|||||||||
73309|Crimson Creek Formation tholeiites|63238|6|Mentioned|p16|||||||||
73346|Crimson Creek Formation volcanics|63167|6|Mentioned|p21|||Informal - see Crimson Creek Formation; refers to volcanics within the formation. ||||||
73310|Crimson Creek Formation""|63238|6|Mentioned|p10|||Informal - see Crimson Creek Formation. ||||||
4899|Crimson Creek Group|22770|5|Briefly described|Fig3 p769||Proterozoic|Misspelt in Figure - should be Crimson Creek Formation which comprises Dreadnought Hill Member, No.1 dolomite and Red Rock Member. See Crimson Creek Formation in text, same page!||||||05-APR-07
4899|Crimson Creek Group|31141|6|Mentioned|p4|||||||||
4899|Crimson Creek Group|41795|6|Mentioned|p49|||||||||
4899|Crimson Creek Group|42227|5|Briefly described|p33, p43|Early Cambrian|Early Cambrian|Overlain by Success Creek Group and correlates. Unfossiliferous sequences of turbiditic siliciclastics and volcanics. Described as being "Eocambrian' in age (Williams 1976).||||||16-JUN-09
4899|Crimson Creek Group|43138|6|Mentioned|p707,Fig.1.|||||||||
4899|Crimson Creek Group|50327|5|Briefly described|p302 Fig. 2|Neoproterozoic|Neoproterozoic|Age: >700-<600Ma.||||||07-FEB-11
4899|Crimson Creek Group|67655|6|Mentioned|p6|||Togari Group correlates include Ahrberg Group, Timbs Group, Success Creek Group, Crimson Creek Group and Weld River Group.||||||
4899|Crimson Creek Group|70025|6|Mentioned|p2|||[Similar to Crimson Creek Formation?]||||||
74078|Crimson Creek basalts|61395|6|Mentioned|p92|||Informal reference to basalts within the Crimson Creek Formation.||||||07-FEB-11
4900|Crimson Creek formation|42178|6|Mentioned|p225|||||||||
4901|Crimson Creek group|39361|6|Mentioned|p1440|||||||||
73345|Crimson Creek volcanics|63167|5|Briefly described|p20|||Informal - see Crimson Creek Formation; refers to volcanics within the formation. ||||||
78875|Crole Hills Diamictite|62903|5|Briefly described|p729, p731|||Tasmania. Age from Calver et al. 2004.|max age 582+/-4 Ma, U-Pb zircon SHRIMP|||correlated with Elatina Formation||
81342|Croles Diamictite|70082|6|Mentioned|p3|||||||||
21579|Croles Hill Mixtite|23191|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Kanunnah Subgroup.||||||05-APR-07
21579|Croles Hill Mixtite|63250|5|Briefly described|p3 Fig. 2, p6-7|||Of the Kanunnah Subgroup (Togari Group). Overlain by Spinks Creek Volcanics. Massive, unbedded, poorly sorted, basaltic diamictite. Possible interpretation of this unit is that it is a glacial diamictite (tillite).||||||
21579|Croles Hill Mixtite|67502|6|Mentioned|p13, p64|||Replaced by Croles Hill Diamictite. Term used by Everard et al. (1996).||||||
21579|Croles Hill Mixtite|73331|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Equivalents of Croles Hill Mixtite may be included in correlate of Keppel Creek Formation map unit.||Togari Group||||
4943|Crotty Quartzite|638|5|Briefly described|p126 Fig. 4.17|Silurian|Silurian|Of the Eldon Group. See also p130 Fig. 4.20.||||||
4943|Crotty Quartzite|31141|4|Described|p5|||||||||
4943|Crotty Quartzite|31174|5|Briefly described|p173|||Part of Eldon Group.||||||05-APR-07
4943|Crotty Quartzite|31648|6|Mentioned|Fig. 2|||Map||||||
4943|Crotty Quartzite|33839|5|Briefly described|p576|||||||||
4943|Crotty Quartzite|33853|6|Mentioned|Fig.1|||Silurian.||||||05-APR-07
4943|Crotty Quartzite|36788|6|Mentioned|p25|||||||||
4943|Crotty Quartzite|36817|6|Mentioned|p46|||||||||
4943|Crotty Quartzite|37047|6|Mentioned|Fig.1|||||||||
4943|Crotty Quartzite|37727|5|Briefly described|p30|||See also p52 and Fig.1.||||||05-APR-07
4943|Crotty Quartzite|38070|6|Mentioned|Fig.8|||See p96.||||||05-APR-07
4943|Crotty Quartzite|40070|4|Described|p17|||||||||
4943|Crotty Quartzite|40136|6|Mentioned|p19|||See also p23.||||||05-APR-07
4943|Crotty Quartzite|41814|6|Mentioned|Map legend|Silurian||||||||
4943|Crotty Quartzite|41896|5|Briefly described|p27|||||||||
4943|Crotty Quartzite|42551|6|Mentioned|Map legend|||||||||
4943|Crotty Quartzite|44135|5|Briefly described|p11, p21|||Of the Eldon Group. Underlies Amber Slate. Max. thickness: 490m. Quartz sandstone and conglomerate lithologies vary in Duck Creek Syncline and in Zeehan area. Macrofossils and worm casts.||||||08-JUL-15
4943|Crotty Quartzite|63170|5|Briefly described|p201, p210, p225 Fig. 6.12|Silurian|Silurian|Of Gill and Banks 1950). Basal unit of the Eldon Group. Overlain by Amber Slate; probably unconformable over Gordon Group. Thickness: 490m. In the Western Tasmania Terrane. Consists of quartz sandstone, conglomerate and mudstone; deeply leached.||||||07-FEB-11
4943|Crotty Quartzite|63244|5|Briefly described|p1|Devonian|Devonian|Basal unit of the Eldon group. Unconformably overlies Gordon limestone (uppermost bed of the Junee group).||||||
4943|Crotty Quartzite|69050|6|Mentioned|p38|Silurian|Silurian|||||Intruded by the Meredith Granite.||
4943|Crotty Quartzite|69850|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Eldon Group.|||Generally pale grey and in part pink, commonly current-bedded, fine- to coarse-grained quartz sandstone with common pebble conglomerate layers; minor interbedded pale green mudstone and siltstone.|
4943|Crotty Quartzite|69851|5|Briefly described|Map legend|||Mentioned as a correlate to an unnamed unit, of fine- to coarse-grained quartz sandstone with minor mudstone beds and some granule conglomerate layers, in the map area.||||||
4943|Crotty Quartzite|69857|5|Briefly described|Map legend|Devonian|Silurian|||Unit in Eldon Group.||||
4943|Crotty Quartzite|69859|5|Briefly described|Map legend|Devonian|Silurian|Unclear from the legend as to whether this unit is a Formation in Eldon or Tiger Range Group.||Unit in Wurawina Supergroup.|||Shallow-marine quartz sandstone and pebble conglomerate.|
4943|Crotty Quartzite|69875|4|Described|p244, p255-256, p258-263|Llandovery|Llandovery|Western Tasmanian Terrane. 490m thick (ranges from 150-1000m). Age inferred from rare fossils (Rostricellula synchoneua, echinoderm ossicles and worm castings). See also Crotty Sandstone (p254) and Crotty Formation (p262-263). Correlatives described.||Basal Eldon Group ||Conformably or disconformably overlies Gordon Group. Possibly stratigraphically equivalent to Gell Quartzite. Underlies Amber Slate.|Commonly herringbone cross-bedded, medium- to coarse-grained quartz sandstone, commonly with weathered green chromite, with minor granule and pebble conglomerate, siltstone and mudstone units.|
4943|Crotty Quartzite|73313|5|Briefly described|Map legend|Devonian|Silurian|Map unit includes Crotty Quartzite and correlates.||Eldon Group||Overlies Gordon Group.|Shallow marine quartz sandstone and pebble conglomerate.|
4943|Crotty Quartzite|73320|6|Mentioned|Map legend|Silurian|Silurian|Western Tasmania. Map unit includes Crotty Quartzite, Gell Quartzite and correlates; single description of shallow marine quartz sandstone and pebble conglomerate. Grouped in either Eldon Group or Tiger Range Group.||||||
4944|Crotty Sandstone|37046|6|Mentioned|Fig.4|||||||||
4944|Crotty Sandstone|44970|14|Not recorded|p77|||||||||
4944|Crotty Sandstone|45018|14|Not recorded|p15|||||||||
4944|Crotty Sandstone|69875|5|Briefly described|p254|||See also references to Crotty Formation (p262) and Crotty Quartzite (p244, p255-256, p258 Fig 5.13, p261-263).||||Disconformably overlies Bubs Hill correlate of Benjamin Limestone.|Sandstone disconformably overlies massive coarse-grained brown secondary dolostone.|
24891|Crotty Sandstones|30277|6|Mentioned|p212|||Refers Hills and Carey 1949.||||||
4954|Crown Hill Andesites""|30278|5|Briefly described|p182|||Refers Solomon (1960)||||||
4954|Crown Hill Andesites""|32794|6|Mentioned|p608|||||||||
4955|Crown Hill andesite|32794|6|Mentioned|p608|||||||||
4955|Crown Hill andesite|64395|5|Briefly described|p172|||Informal name. Hornblende-phyric andesite occurring mainly as intrusives within the upper part of southern Central Volcanic Complex; together with Reservoir and Anthony Road andesites these form Suite 2 of Mount Read Volcanics.||||||07-FEB-11
4955|Crown Hill andesite|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Central Mount Read Volcanics, with Ar-Ar hornblende age of 489+\-18 Ma.|489+\-18 Ma|||||
4956|Crown Hill andesites|35844|6|Mentioned|p56|||Refers Solomon 1960. Informal name.||||||24-MAY-07
4957|Crown Hill porphyries|30278|6|Mentioned|p183|||Correlation||||||
5045|Curdies Formation|22944|5|Briefly described|Fig3|||||||||
5045|Curdies Formation|23818|5|Briefly described|p164|Late Cretaceous|Late Cretaceous|Underlying unit: Paaratte Formation.||||||
5045|Curdies Formation|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group.  Geological Basin: Otway Basin.||||||
5045|Curdies Formation|24562|5|Briefly described|p3 Table 1|||Geological Province: Otway Basin.||||||
5045|Curdies Formation|29697|6|Mentioned|Fig.11|||||||||
5045|Curdies Formation|29856|5|Briefly described|p38|||||||||
5045|Curdies Formation|30499|6|Mentioned|p98|||||||||
5045|Curdies Formation|30754|6|Mentioned|p12|||Stratigraphic table||||||
5045|Curdies Formation|31245|6|Mentioned|p84|||U.Cretaceous.||||||
5045|Curdies Formation|31372|6|Mentioned|Fig. 2|||||||||
5045|Curdies Formation|31424|6|Mentioned|p32|||Sedimentology||||||
5045|Curdies Formation|31624|6|Mentioned|p96|||U.Cret. Unit of Sherbrook Gp.||||||
5045|Curdies Formation|31625|6|Mentioned|Fig. 5.2|||U.Cretaceous||||||
5045|Curdies Formation|31920|6|Mentioned|p51|||See also Table 3-2,3. U.Cret.||||||
5045|Curdies Formation|32344|6|Mentioned|Fig.2|||||||||
5045|Curdies Formation|32896|6|Mentioned|Encl.7.1.|||U.Cret.||||||
5045|Curdies Formation|32898|6|Mentioned|Table 2-1|||||||||
5045|Curdies Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
5045|Curdies Formation|33936|6|Mentioned|Fig.6|||U.Cret.||||||
5045|Curdies Formation|34063|6|Mentioned|p3|||Table. U.Cret.||||||
5045|Curdies Formation|34308|5|Briefly described|Fig.85|||U.Cret.||||||
5045|Curdies Formation|34611|5|Briefly described|p164|||Fig.80. Upper Cretaceous||||||
5045|Curdies Formation|34987|6|Mentioned|p172|||||||||
5045|Curdies Formation|35722|6|Mentioned|p3|||Stratigraphy.||||||
5045|Curdies Formation|38625|6|Mentioned|Table 2|||||||||
5045|Curdies Formation|40003|5|Briefly described|p43|||See also Fig.10||||||
5045|Curdies Formation|41016|5|Briefly described|p214|||||||||
5045|Curdies Formation|41185|6|Mentioned|p177|||||||||
5045|Curdies Formation|41704|6|Mentioned|p100|||||||||
5045|Curdies Formation|41868|5|Briefly described|p534|||||||||
5045|Curdies Formation|41936|6|Mentioned|p75|||||||||
5045|Curdies Formation|42361|6|Mentioned|p17|||Used 1966 to 1988 but rejected 1971 because Timboon Sand/Sst had priority & definition confused.||||||
5045|Curdies Formation|42524|5|Briefly described|Fig.3 P27|||||||||
5045|Curdies Formation|42555|6|Mentioned|p285|||||||||
5045|Curdies Formation|42827|5|Briefly described|p533|||||||||
5045|Curdies Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5045|Curdies Formation|43590|6|Mentioned|p14|||Replaced by Timboon Sand Member||||||
5045|Curdies Formation|43660|6|Mentioned|Fig.6,p15||Late Cretaceous|||||||
5045|Curdies Formation|43783|6|Mentioned|Fig14, p11||Late Cretaceous|||||||
5045|Curdies Formation|43784|6|Mentioned|Fig10, p12||Late Cretaceous|||||||
5045|Curdies Formation|48911|3|Fully described|p22|||U. Cret.||||||
5045|Curdies Formation|48977|6|Mentioned|Fig.5|||||||||
5045|Curdies Formation|49060|5|Briefly described|Fig.33|||||||||
5045|Curdies Formation|61182|6|Mentioned|p19|||Of Reynolds et al (1966). Preferred term is Timboon Sand Member, replacing this name due to confusion in its definition. See also Curdies Beds. ||||||
5045|Curdies Formation|63124|5|Briefly described|p48 Fig. 5.1|||Of Reynolds et al (1966) and Williamson et al (1987). Superseded Timboon Sandstone Member; superseded by Curdies Beds, then Timboon Sand; now called Timboon Sandstone. Geological Province: Otway Basin.||||||
5079|Currawong Formation|41793|5|Briefly described|p58|||||||||
74648|Currie Granite|64400|5|Briefly described|p2 Fig. 1b|Neoproterozoic|Neoproterozoic|Age: 748+/-2Ma.||||||07-FEB-11
73311|Curtain Davis basalts|63238|5|Briefly described|p18|||Informal name for basalts in the Montezuma Falls area - which appear to lie within the Tyndall Group correlates.  ||||||
30400|Curtin Davis Volcanics|43133|6|Mentioned|p601|||Variation on Curtin-Davis Volcanics.||||||
5091|Curtin Davis Volcanics""|35791|6|Mentioned|p226|||||||||
73273|Curtin-Davis volcanics|63169|6|Mentioned|p161|||Informal name for volcanics occurring along the western flank of the Mount Read belt.||||||
73273|Curtin-Davis volcanics|63240|6|Mentioned|p4|||||||||
73273|Curtin-Davis volcanics|69874|5|Briefly described|p161, p168|Middle Cambrian|Middle Cambrian|Rosebery to Mt Cattley area, west of Hercules. Poorly exposed/known. Also appears as Curtin Davis Volcanics on p168.||||Hosted within probable Tyndall Group.|Very altered vesicular lavas, breccias, volcaniclastics; andesitic.|
5104|Cygnet Alkaline Complex|37818|6|Mentioned|Table 3|||||||||
5104|Cygnet Alkaline Complex|43870|14|Not recorded|p345|||Late early Cretaceous.||||||05-MAY-22
5104|Cygnet Alkaline Complex|65645|3|Fully described|p3-23|Cretaceous|Cretaceous|Around Cygnet, and between Oyster Cove, Kettering and Woodbridge.|95-99 Ma K/Ar.||||Syenite and related alkaline rocks as dykes, sills, sheets and possible stocks.|30-MAR-12
5104|Cygnet Alkaline Complex|69879|4|Described|p453-459, p462|Cretaceous|Cretaceous|Located at Cygnet near Huon River. Associated with gold and minor base metal mineralisation. Severe thermal effects on intruded sedimentary rocks. Geochemistry, petrogenesis, comparisons, mineralisation and alteration described in detail. May be source of volcanogenic material in Otway Group (Bass Basin) and Strzelecki Group (Gippsland Basin). Geochronology by Evernden and Richards (1962). McDougall and Leggo (1965) determined hornblende K-Ar ages of 100 and 97 Ma.|101 Ma (K-Ar sanidine and biotite).|||Intrudes Lower Parmeener Supergroup, Jurassic dolerite, Bundella Formation, Woody Island Formation, Truro Tillite.|Syenite intrusive complex: large sheet-like intrusions, stocks, narrow sills and dykes. Two broad types: silica-oversaturated 'syenite porphyry' intrusions, cut by silica-undersaturated 'sanidine porphyry'.|
5104|Cygnet Alkaline Complex|73369|6|Mentioned|p332|||||||||
5107|Cygnet Complex|24164|5|Briefly described|p17|Early Cretaceous|Early Cretaceous|Lies on edge of Tasmania Basin.|~100 Ma, McDougall and Leggo 1965||||Highly magnetic|
5107|Cygnet Complex|30661|6|Mentioned|Table 1|||||||||
74578|Cygnet Formation|63868|6|Mentioned|p20|||Informal reference to Cygnet Coal Measures.||||||07-FEB-11
31906|Cygnet Intrusive Complex|43870|14|Not recorded|p276|||Late early Cretaceous||||||
5108|Cygnet Syenite complex|37406|6|Mentioned|p88|||||||||
5109|Cygnet akaline complex|30312|6|Mentioned|p59|||Misspelling of Cygnet alkaline complex [CEBMar95]||||||
5110|Cygnet alkaline complex|36019|6|Mentioned|Plate 9|||||||||
5110|Cygnet alkaline complex|37818|6|Mentioned|p82|||||||||
5110|Cygnet alkaline complex|40263|6|Mentioned|Table 2|||[Originally entered for NSW. CEBMar95]||||||
5110|Cygnet alkaline complex|63592|6|Mentioned|p31|||Informal name. See also the informal Cygnet complex and Cygnet porphyry complex.||||||03-OCT-07
5111|Cygnet coals|41911|6|Mentioned|p146|||||||||
5112|Cygnet complex|32106|6|Mentioned|p306|||Palaeomagnetic data||||||
5112|Cygnet complex|33354|6|Mentioned|p180|||Refs. Robertson & Hastie (1962).||||||
5112|Cygnet complex|63592|5|Briefly described|p9|Cretaceous|Cretaceous|Informal name. Age: 109-95Ma (Evernden and Richards, 1962; McDougall and Leggo, 1965). Probably related to the inititaion of the Antarctic-Atlantic rift at about 97Ma.||||||31-JAN-08
73659|Cygnet porphyry complex|63592|5|Briefly described|p4 (Abstract)|||Informal name. Alkaline intrusive complex with gold mineralisation.||||||03-OCT-07
73661|Cygnet suite|63592|6|Mentioned|p31|||Informal reference to the alkaline intrusive complex also referred to as Cygnet  porphyry complex and Cygnet complex.||||||31-JAN-08
5122|Dabool Formation|24549|4|Described|p7|Permian|Permian|Of the Woodbridge Group. Max. Thickness: 40ft. Consists of medium quartz and feldspar grains in a mudstone matrix, rich brachiopod fauna.||||||10-APR-07
5122|Dabool Formation|30156|5|Briefly described|p39|||Mainly Fossil content.||||||06-FEB-08
5122|Dabool Formation|32627|6|Mentioned|p29|Permian|Permian|Informally named in the Dabool-Weston-Garcia Formations grouping in stating that these units have "generally not been separated during mapping".||||||21-MAY-08
5122|Dabool Formation|33711|6|Mentioned|Table 1|||||||||
5122|Dabool Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Upper Permian. Of the Woodbridge Group.  Brachiopod sandstone.||||||06-FEB-08
5122|Dabool Formation|63172|5|Briefly described|p305|||Poorly sorted sandstone conglomerate intervals. In Central Plateau area of Tasmania.||||||07-FEB-11
5122|Dabool Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
5133|Dalcoath Granite|31179|6|Mentioned|p364|||||||||
5134|Dalcoath Member|22770|4|Described|Fig3p769|Neoproterozoic|Neoproterozoic|Laminated siltstone within the Success Creek Group. Figure shows type section of Renison mine.||||||10-APR-07
5134|Dalcoath Member|33218|5|Briefly described|p37|||||||||
5134|Dalcoath Member|64394|5|Briefly described|p98|||Member has identifiable upper units informally named Dalcoath Contorted (up to 80m)intensely contorted, laminated, black-grey shale+siltst); overlain by Dalcoath Upper (10-15m) of laminated shale-siltstone with thin, folded, boudined/nodular dolomite beds||||||05-NOV-08
5134|Dalcoath Member|69876|5|Briefly described|p352|||Renison Bell mine.||Success Creek Group.|||Siltstones, shales, sandstones, quartzites.|
5136|Dalcoath Quartzite|32409|5|Briefly described|p582|||||||||
5136|Dalcoath Quartzite|37053|5|Briefly described|p394|||||||||
5136|Dalcoath Quartzite|38261|6|Mentioned|p203|||||||||
5135|Dalcoath Quartzite""|41795|6|Mentioned|p23|||||||||
37072|Dalcoath granite|23718|6|Mentioned|p75|||Misspelt||||||
5148|Dally Siltstone|30889|6|Mentioned|p23|||Contained within the structural Cambrian slice known as Middle Arm Creek Slice.||||||10-APR-07
35654|Dally's Siltstone|23114|5|Briefly described|p468|||||||||
35654|Dally's Siltstone|61395|6|Mentioned|p29, p34|||Superseded by Dallys Siltstone. Described as being overlain by and interfingered with Blyths Creek Formation by Green (1959) - but it is now concluded that they are are a part of Blyths Creek Formation.||||||07-FEB-11
5149|Dallys Siltstone""|36380|6|Mentioned|p219|||Contains Middle Cambrian fauna.||||||10-APR-07
5154|Dalmayne conglomerate|41855|6|Mentioned|Plate 17|||||||||
78861|Darlington Formation|67543|6|Mentioned|p145 Fig.4|||Presented as Darlington Fm. in figure.|||||Limestone.|
5226|Darlington Limestone Formation|30819|6|Mentioned|p108|||||||||
5227|Darlington limestone|38197|6|Mentioned|p684|||||||||
5241|Dartmoor Formation|23671|5|Briefly described|p2|||Disconformably overlain by the Knight Group.||||||
5241|Dartmoor Formation|23818|4|Described|p174 Fig.84, p175|Late Paleocene|Late Paleocene|Of the Knight Group. Geological Province: Otway Basin. Underlain by Bahgallah Formation. Max. thickness: 1541 ft.||||||10-APR-07
5241|Dartmoor Formation|24551|6|Mentioned|p295|||||||||
5241|Dartmoor Formation|29697|6|Mentioned|Fig.11|||||||||
5241|Dartmoor Formation|30514|6|Mentioned|p108|||||||||
5241|Dartmoor Formation|30754|6|Mentioned|p14|||Stratigraphic table||||||
5241|Dartmoor Formation|30932|6|Mentioned|Map legend|Eocene|Paleocene|Equivalent Dilwyn Formation, Palaeocene - Eocene||||||
5241|Dartmoor Formation|31372|6|Mentioned|Fig. 2|||||||||
5241|Dartmoor Formation|31424|6|Mentioned|p32|||Sedimentology||||||
5241|Dartmoor Formation|31624|2|Defined|p99|Paleocene|Paleocene|Unit of Knight Gp. See also P101||||||
5241|Dartmoor Formation|31625|6|Mentioned|Fig. 5.2|||Palaeocene - Eocene||||||
5241|Dartmoor Formation|31629|6|Mentioned|Fig. 5.1|||U. to M. Palaeocene||||||
5241|Dartmoor Formation|31920|4|Described|p52|||Palaeocene. See also P55, Figs 3-2,3,4,5.||||||
5241|Dartmoor Formation|31922|6|Mentioned|Table 2|||||||||
5241|Dartmoor Formation|32117|6|Mentioned|Fig.2|||||||||
5241|Dartmoor Formation|32574|6|Mentioned|p76|||||||||
5241|Dartmoor Formation|32852|6|Mentioned|p18|||||||||
5241|Dartmoor Formation|32894|4|Described|p287|||U.Palaeocene||||||
5241|Dartmoor Formation|32897|6|Mentioned|p180|||||||||
5241|Dartmoor Formation|33109|5|Briefly described|p86|||Geological section||||||
5241|Dartmoor Formation|33319|6|Mentioned|p176|||Fauna||||||
5241|Dartmoor Formation|33940|6|Mentioned|p414|||||||||
5241|Dartmoor Formation|34308|5|Briefly described|p175|||See also Fig.84. Correlation chart. Wangerripian||||||
5241|Dartmoor Formation|34418|6|Mentioned|p503|||||||||
5241|Dartmoor Formation|35066|6|Mentioned|p202|||||||||
5241|Dartmoor Formation|35722|6|Mentioned|p4|||Stratigraphy.||||||
5241|Dartmoor Formation|37548|6|Mentioned|p129|||||||||
5241|Dartmoor Formation|38068|6|Mentioned|Fig.7|||||||||
5241|Dartmoor Formation|38070|6|Mentioned|Fig.12|||Otway Basin||||||
5241|Dartmoor Formation|39408|6|Mentioned|Fig.5|||||||||
5241|Dartmoor Formation|42827|6|Mentioned|p276|||||||||
5241|Dartmoor Formation|48624|14|Not recorded|p4,Fig.2|||Fm. of Knight Gp. (J54-6/Benara).||||||
5241|Dartmoor Formation|48911|6|Mentioned|Chart 1|||||||||
5241|Dartmoor Formation|61155|5|Briefly described|p18|Early Eocene|Late Paleocene|Of the Wangerrip (Knight) Group. Overlies Bahgallah Formation. Max. thickness: 500m. Geological Province: Otway Basin (Gambier Embayment).||||||03-MAR-10
5244|Dartmoor Sand|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
5244|Dartmoor Sand|24551|6|Mentioned|p292|||Of the Wangerrip Group.||||||
5244|Dartmoor Sand|35285|6|Mentioned|p414|||||||||
5244|Dartmoor Sand|41185|6|Mentioned|Fig.4|||||||||
5244|Dartmoor Sand|41704|6|Mentioned|Fig.3|||||||||
5244|Dartmoor Sand|42524|5|Briefly described|Fig.3 P27|||||||||
5244|Dartmoor Sand|42555|5|Briefly described|Fig.2 P285|||||||||
5244|Dartmoor Sand|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5244|Dartmoor Sand|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
5255|Darwin Glass|45087|5|Briefly described|p243|||Chem. analyses.||||||
5255|Darwin Glass|69880|5|Briefly described|p530-531|Pleistocene|Pleistocene|Occurs across c.410 km2 to the SW, W and NW of Darwin Crater, 25km S of Queenstown. Recognised by Ford (1972), although the glass was familiar to early explorers and widely used as implements by Aboriginals throughout western Tasmania. Formed from impact melting of Siluro-Devonian sandstone and slaty mudstone. |816 +/- 7 ka (Ar: Lo et al., 2002).||||Typically black to grey, brown or green siliceous glass, with some surface ropy and splashform textures.|
5257|Darwin Keratophyre""|30278|6|Mentioned|p175|||Refers Solomon(1964)||||||
70181|Darwin glass|61560|5|Briefly described|p499|Neoproterozoic|Neoproterozoic|Informal name. Siliceous impact glass found over a strewn field in western Tasmania. Contains embedded coesite. Age: 815-796Ma.||||||
40332|Darwin granite|23940|6|Mentioned|p915|||||||||
40332|Darwin granite|70274|4|Described|p447-448|Cambrian|Cambrian|Granitic body found within the central Mount Read Volcanics. Intrudes Western Volcano-Sedimentary Sequences, Central Volcanic Complex, and Eastern Quartz-Phyric Sequence. Interpreted as subvolcanic intrusions genetically related to the host volcanic successions (Large et al., 1996), and may have played important roles in driving hydrothermal circulation that formed VHMS deposits in the belt (Large et al., 1996; Huston et al., 2011).|||||Medium-grained quartz + K-feldspar + plagioclase + biotite + hornblende+\-apatite+\-zircon+\-rutile granite or granodiorite.|
73333|Dasher River Andesite|63249|5|Briefly described|p2|Cambrian|Cambrian|Of Corbett (pers.comm.) He considered this should be added to the Cambrian volcanics grouping of Gog Range district, for andesites north of Dasher River, and overlying Gog Range Greywacke. However,  this interpretation is not universally accepted.||||||
73334|Dasher River Andesites|63249|5|Briefly described|p3|||Probably misspelt and should be Dasher River Andesite. ||||||
5270|Davey Group""|41795|6|Mentioned|p17|||||||||
5270|Davey Group""|63168|6|Mentioned|p50 Tb. 3.1|||Of Taylor (1954). Informal version - see Davey Group. ||||||
73442|Davey System|63168|6|Mentioned|p50 Tb. 3.1|||Historical name for Davey Group (Carey 1947c).||||||16-JUL-07
24907|David formation|41993|6|Mentioned|p7|||||||||
5318|Deep Creek Basic Volcanic Formation|30294|5|Briefly described|p866|||||||||
5320|Deep Creek Basic Volcanics|30293|6|Mentioned|p629|||||||||
5319|Deep Creek Basic Volcanics Formation|30293|6|Mentioned|p629|||||||||
73443|Deep Creek Volcanics""|63168|6|Mentioned|p57, p64|||Informal name (of Cox 1968; Cox and Glasson 1971; Collins 1983) for the largest concentration of basalt in the Cleveland-Waratah area in the vicinity of the Cleveland Mine.||||||
24911|Deep Creek basic volcanics|33218|5|Briefly described|p27|||||||||
5332|Deep Glen Bay Adamellite|39680|6|Mentioned|Map legend|Devonian|Devonian|||||||
5333|Deep Glen Bay granite|35819|6|Mentioned|p10|||||||||
74133|Deloraine basalts|32627|5|Briefly described|p41|Tertiary|Tertiary|Not intended as a formal name.  Age is Tertiary. Described by Wells (1957) - who differentiated two major basalt types: Ashley Basalt and its member, Exton Member. See these two units for more detail on petrology.||||||07-FEB-08
5362|Demons Bluff Formation|22674|5|Briefly described|Fig.2 p719|Late Eocene|Middle Eocene|||||||
5362|Demons Bluff Formation|22756|6|Mentioned|P30|||||||||
5362|Demons Bluff Formation|22875|3|Fully described|p62|Early Oligocene|Middle Eocene|Of the Nirranda Group.||||||31-JAN-07
5362|Demons Bluff Formation|22944|5|Briefly described|Fig3|Oligocene|Eocene|||||||
5362|Demons Bluff Formation|23230|4|Described|Table4-1p40, 42, 44|Oligocene|Eocene|Present in the Torquay Basin.||||||
5362|Demons Bluff Formation|23240|5|Briefly described|p120-1|Late Oligocene|Eocene|||||||
5362|Demons Bluff Formation|23307|5|Briefly described|Map Legend|Oligocene|Eocene|Of Nirranda Group||||||
5362|Demons Bluff Formation|23322|5|Briefly described|957 Fig.2|Oligocene|Eocene|Of the Nirranda Group.  Geological Province: Otway Basin.||||||07-SEP-09
5362|Demons Bluff Formation|23372|4|Described|p249-250,253,257,259||Eocene|In the Bass Basin.||||||31-JAN-07
5362|Demons Bluff Formation|23768|5|Briefly described|p28 Fig.5|Early Miocene|Oligocene|In Torquay/Geelong area.||||||11-SEP-09
5362|Demons Bluff Formation|23778|5|Briefly described|p660-661|||Now known as Demons Bluff Group - introduced by Trupp et al (1994). Geological Province: Torquay Basin.||||||31-JAN-07
5362|Demons Bluff Formation|24038|5|Briefly described|p443|||||||||
5362|Demons Bluff Formation|24055|5|Briefly described|p74|Tertiary|Tertiary|Of Eastern Coal Measures.  Geological Basin: Bass Basin.||||||
5362|Demons Bluff Formation|24369|5|Briefly described|p60|Late Paleocene|Late Paleocene|Geological Province: Bass Basin.||||||24-FEB-05
5362|Demons Bluff Formation|24551|5|Briefly described|p246|Oligocene|Eocene|Of the Nirrandra Group.||||||
5362|Demons Bluff Formation|24562|5|Briefly described|p8 Fig. 2|Eocene|Eocene|Of the Nirranda Group.  Geological Province: Otway Basin. Maximum Thickness: 277m.||||||
5362|Demons Bluff Formation|29355|6|Mentioned|p190|||||||||
5362|Demons Bluff Formation|29356|6|Mentioned|p147|||Stratigraphy.||||||
5362|Demons Bluff Formation|29823|6|Mentioned|p14|||||||||
5362|Demons Bluff Formation|29885|6|Mentioned|p427|||||||||
5362|Demons Bluff Formation|30576|6|Mentioned|Table 2|||||||||
5362|Demons Bluff Formation|30929|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
5362|Demons Bluff Formation|31245|4|Described|p82|||||||||
5362|Demons Bluff Formation|31624|5|Briefly described|p105|||Lithology||||||
5362|Demons Bluff Formation|31922|6|Mentioned|p169|||||||||
5362|Demons Bluff Formation|32162|6|Mentioned|Fig.3|||Correlation chart||||||
5362|Demons Bluff Formation|32574|6|Mentioned|p77|||||||||
5362|Demons Bluff Formation|32893|5|Briefly described|p48|||Spore-pollen assemblages||||||
5362|Demons Bluff Formation|33155|6|Mentioned|p117|||||||||
5362|Demons Bluff Formation|33228|6|Mentioned|p2|||||||||
5362|Demons Bluff Formation|33240|6|Mentioned|p2|||||||||
5362|Demons Bluff Formation|34063|6|Mentioned|p10|||U.Eocene. Table||||||
5362|Demons Bluff Formation|34655|6|Mentioned|p299|||||||||
5362|Demons Bluff Formation|35013|6|Mentioned|p395|||||||||
5362|Demons Bluff Formation|35066|3|Fully described|p221|||||||||
5362|Demons Bluff Formation|35151|6|Mentioned|p150|||||||||
5362|Demons Bluff Formation|35276|3|Fully described|p231|||||||||
5362|Demons Bluff Formation|35290|4|Described|p29|||See also p25.||||||31-JAN-07
5362|Demons Bluff Formation|35854|6|Mentioned|p160|||||||||
5362|Demons Bluff Formation|36499|3|Fully described|p38|||||||||
5362|Demons Bluff Formation|37129|6|Mentioned|p359|||||||||
5362|Demons Bluff Formation|37131|6|Mentioned|p364|||||||||
5362|Demons Bluff Formation|41043|6|Mentioned|p96|||||||||
5362|Demons Bluff Formation|41124|4|Described|p255|||||||||
5362|Demons Bluff Formation|41185|6|Mentioned|Fig.4|||||||||
5362|Demons Bluff Formation|41201|5|Briefly described|p2|||||||||
5362|Demons Bluff Formation|41642|6|Mentioned|Fig.8.6|||||||||
5362|Demons Bluff Formation|41704|6|Mentioned|Fig.3|||||||||
5362|Demons Bluff Formation|41715|6|Mentioned|p312|||||||||
5362|Demons Bluff Formation|41868|5|Briefly described|p545|||See also p581.||||||31-JAN-07
5362|Demons Bluff Formation|42184|6|Mentioned|Fig.2 P348|||||||||
5362|Demons Bluff Formation|42318|6|Mentioned|p6|||||||||
5362|Demons Bluff Formation|42452|5|Briefly described|Map legend|late Oligocene|late Eocene|||||||
5362|Demons Bluff Formation|42453|4|Described|p14|late Oligocene|late Eocene|||||||
5362|Demons Bluff Formation|42524|5|Briefly described|Fig.3 P27|||||||||
5362|Demons Bluff Formation|42827|3|Fully described|p305|||||||||
5362|Demons Bluff Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
5362|Demons Bluff Formation|43171|6|Mentioned|5-8|||Of Nurranda Group. Age: 35-40Ma||||||
5362|Demons Bluff Formation|43208|5|Briefly described|map legend|Early Oligocene|Middle Eocene|||||||
5362|Demons Bluff Formation|43219|5|Briefly described|Fig.3,p6.|Oligocene|Eocene|Of the Nirranda Group.||||||31-JAN-07
5362|Demons Bluff Formation|43590|4|Described|p23|Early Oligocene|Middle Eocene|||||||
5362|Demons Bluff Formation|43660|6|Mentioned|Fig.6,p15|Oligocene|Eocene|||||||
5362|Demons Bluff Formation|43702|6|Mentioned|Fig.2,p398|Late Oligocene|Late Eocene|||||||
5362|Demons Bluff Formation|43733|6|Mentioned|Fig.2.11,p65|Oligocene|Eocene|||||||
5362|Demons Bluff Formation|43744|6|Mentioned|Fig.3,p3|||||||||
5362|Demons Bluff Formation|43937|5|Briefly described|Map Legend|Middle Eocene|Paleocene|||||||
5362|Demons Bluff Formation|44135|5|Briefly described|p47|Late Eocene|Middle Eocene|Overlain by Torquay Group. Thickness: 40m. Geological province: Durroon Basin. Mainly sandstone in this basin.||||||07-DEC-09
5362|Demons Bluff Formation|46988|6|Mentioned|p201|||||||||
5362|Demons Bluff Formation|48831|14|Not recorded|p.10,13|||||||||
5362|Demons Bluff Formation|48911|6|Mentioned|p49|||Chart 1||||||
5362|Demons Bluff Formation|61155|5|Briefly described|p3, p18|Early Oligocene|Middle Eocene|Includes the Angahook Member. Overlies Eastern View Formation; overlain by Torquay Group (Jan Juc Formation). Partly interfingers with Mepunga Formation. Max. thickness: 170m in Otway Basin and 280m in Bass Basin. Geological Province: Bass Basin.||||||03-MAR-10
5362|Demons Bluff Formation|61182|3|Fully described|p27, p23, p24|Early Oligocene|Middle Eocene|Part of Nirranda Gp (Port Campbell Embayment area). Interbedded with pillow basalt and pyroclastics of main Older Volcanics plug. Overlies Eastern View Fm/Wangerrip Gp; underlies Clifton Fm or Gellibrand Marl; interfingers with Mepunga Fm. towards coast..||||||06-JAN-10
5362|Demons Bluff Formation|61624|6|Mentioned|p466 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
5362|Demons Bluff Formation|61626|5|Briefly described|p486 Fig. 2|Oligocene|Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
5362|Demons Bluff Formation|61628|5|Briefly described|p509 Fig. 3|Early Oligocene|Middle Eocene|Of Nirranda Group. Geological Province: Otway Basin.||||||07-APR-09
5362|Demons Bluff Formation|63173|5|Briefly described|p342 Fig. 9.2, p349 |Late Oligocene|Late Eocene|Overlies Eastern View Group. Geol.prov: Bass Basin. Marine claystone, siltstone + sandstone; carbonaceous/bioturbated.Thickness: >270m. Uppermost part correlates with Lakes Entrance Fm, the regional sealing unit in Gippsland Basin.||||||07-FEB-11
5362|Demons Bluff Formation|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||Nirranda Group.||||
5362|Demons Bluff Formation|63445|5|Briefly described|Map legend.|Eocene|Eocene||||||Marine: silt, clay, carbonaceous, pyritic, burrowed.|
5362|Demons Bluff Formation|65316|5|Briefly described|p596-7, p602 Fig 5|Rupelian||Defined 1952 (Raggatt and Crespin). Now known as the Demons Bluff Group; renamed by Trupp et al. in 1994.||||Underlies the Point Addis Limestone and Jan Juc Marl.||23-APR-12
5362|Demons Bluff Formation|65715|5|Briefly described|p11 Tb.7|||Used by Raggatt and Crespin (1955). Superseded name for Demons Bluff Group.||||||06-FEB-15
5362|Demons Bluff Formation|66002|5|Briefly described|p10 Tb.7, p12, p26 Fig.7|||Used by Raggatt and Crespin (1955) and more recently. Was part of Nirranda Group. Superseded name for Demons Bluff Group. Silt, fine sand, clay, clayey sand, carbonaceous, pyritic, burrowed. Contains arenaceous foraminifers||||||
5362|Demons Bluff Formation|66245|6|Mentioned|p6 Fig.5. |Priabonian|Lutetian|||Unit in Nirranda Group.||||
5362|Demons Bluff Formation|67367|5|Briefly described|p131 Fig.2. |Late Eocene|Middle Eocene|||Unit in Nirranda Group.||||
5362|Demons Bluff Formation|69651|5|Briefly described|p10|Oligocene|Eocene|||Nirranda Group.||Overlies Dilwyn Formation unconformably and Eastern View Formation. Is overlain unconformably by Clifton Formation.||
5362|Demons Bluff Formation|69879|4|Described|p435-436|Oligocene|Eocene|Regional seal for hydrocarbon reservoirs. Overlies extrusive alkali olivine basalt, transitional to olivine-bearing tholeiites.||Demons Bluff Sequence||Possibly overlies Anglesea Formation unconformably.|Marine shale.|
5362|Demons Bluff Formation|69881|5|Briefly described|p563|||Bass Basin. Shales of this unit seal hydrocarbon reservoirs in Eastern View Group.||||Overlies Eastern View Group, regionally.|Marine shale.|
5362|Demons Bluff Formation|70077|6|Mentioned|Regional: p5|||Onshore NE Otway Basin and Torquay Sub-basin.||||||
5362|Demons Bluff Formation|70880|6|Mentioned|p77|Oligocene|Eocene|Otway Basin.||||||
5362|Demons Bluff Formation|71266|6|Mentioned|p614 Fig.3|Oligocene|Eocene|Otway Basin.||||||
5362|Demons Bluff Formation|73357|5|Briefly described|p28-29, p44|Priabonian|Lutetian|Otway Basin, Gellibrand Trough. Nothofagidites asperus Spore-Pollen Zone documented from Demons Bluff Formation, non-marine to nearshore marine depositional environments. Correlated to Corrudinium incompositum Dinocyst Zone, and the Achilleodinium biformoides Dinocyst Zone, nearshore marine depositional environment.||||Overlies Eastern View Formation, underlies Narrawaturk Marl.||
5362|Demons Bluff Formation|73383|5|Briefly described|p3|Oligocene|Eocene|Otway Basin.||Nirranda Group||Overlies Wangerrip Group, underlies Heytesbury Group|Sandstones, mudstones.|
5362|Demons Bluff Formation|73385|5|Briefly described|p5|Oligocene|Eocene|Otway Basin.||Nirranda Group|||Marginal marine and lower coastal plain sandstones, mudstones.|
5362|Demons Bluff Formation|73486|6|Mentioned|p511 Fig.2|Rupelian|Lutetian|Otway Basin.||Nirranda Group||||
5362|Demons Bluff Formation|73594|6|Mentioned|p4|Oligocene|Eocene|Otway Basin.||Nirranda Group||||
80013|Demons Bluff Shale""|69297|5|Briefly described|p144,|||Durroon Sub-basin, Bass Basin. Is considered to be the regional seal of the Bass Basin.
Uppermost unit of the Flinders Sequence.|||||Thin and relatively coarse-grained shale. |19-SEP-17
73124|Denison Group, lower|44135|6|Mentioned|p28|||Informal - see Denison Group. Western Tasmanian rocks that correlate with Cabbage Tree Formation.||||||07-DEC-09
73124|Denison Group, lower|61395|6|Mentioned|p15|||Informal - see Denison group.||||||07-FEB-11
5371|Denison Range conglomerate and quartzite|30275|6|Mentioned|p114|||Refers Ward(1910)||||||
27388|Denison Sub-Group|36379|6|Mentioned|p202|||||||||
27388|Denison Sub-Group|37412|6|Mentioned|p28|||||||||
27388|Denison Sub-Group|39235|6|Mentioned|Map legend|Ordovician|Late Cambrian|Late Cambrian to Ordovician||||||
27388|Denison Sub-Group|41142|6|Mentioned|Fig.1|||||||||
27388|Denison Sub-Group|41693|6|Mentioned|Map legend|||||||||
27388|Denison Sub-Group|41694|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27388|Denison Sub-Group|41795|3|Fully described|p44|||||||||
27388|Denison Sub-Group|69851|5|Briefly described|Map legend|||Mentioned as a correlate to two unnamed units (conglomerate, and sandstone-siltstone) in the map area which are also stated to be correlates to Mount Zeehan Conglomerate and Moina Sandstone.||||||
5373|Denison Sub-group|36047|4|Described|p364|||||||||
5373|Denison Sub-group|40127|6|Mentioned|p10|||||||||
5373|Denison Sub-group|40136|6|Mentioned|p23|||||||||
5375|Denison Subgroup|23718|4|Described|p19|||See also pages 11, 60.||||||
5375|Denison Subgroup|30275|2|Defined|p112|Late Cambrian|Late Cambrian|Middle Late Cambrian to Early Ordovician age||||||
5375|Denison Subgroup|30279|6|Mentioned|p123|||||||||
5375|Denison Subgroup|30281|5|Briefly described|p10|||||||||
5375|Denison Subgroup|35853|6|Mentioned|Fig.1|||Stratigraphic column showing range of conodontophorids.||||||
5375|Denison Subgroup|35860|6|Mentioned|Fig.1|||||||||
5375|Denison Subgroup|37408|6|Mentioned|Fig.1|||||||||
5375|Denison Subgroup|37801|6|Mentioned|p113|||||||||
5375|Denison Subgroup|39976|6|Mentioned|p101|||||||||
5375|Denison Subgroup|40708|6|Mentioned|p95|||||||||
5375|Denison Subgroup|41793|6|Mentioned|p46|||See also P39||||||
5375|Denison Subgroup|42478|6|Mentioned|p5|||Used 1975. Superseded by Denison Group.||||||
5375|Denison Subgroup|43668|6|Mentioned|p5|||||||||
5375|Denison Subgroup|45130|6|Mentioned|p15|||||||||
5374|Denison Subgroup siliciclastics|37408|6|Mentioned|Fig.1|||||||||
37542|Denison group|23309|6|Mentioned|p359|||Informal name.||||||11-APR-07
83698|Dennison Supergroup|73430|5|Briefly described|p518|Early Ordovician|Late Cambrian|Latest Cambrian to Earliest Ordovician age. Post-Delamerian.|||Jukes Conglomerate, Owen Conglomerate|Unconformably overlies Mount Read Volcanics, Tyndal Group|Includes molassic conglomerates.|
5409|Derwent Beds|48971|6|Mentioned|p89|||||||||
81326|Detention Metaquartzite|70025|6|Mentioned|p11|||Rocky Cape Zone. ||Unit of Rocky Cape Group.||||
5420|Detention Quartzite|42358|6|Mentioned|p18, p12|||Shown in brackets after Detention Subgroup.  Intended usage unclear.||||||
5420|Detention Quartzite|69849|5|Briefly described|Map legend|||Age given as Precambrian.||Unit in Rocky Cape Group.||Overlies Cowrie Siltstone. Is overlain by Irby Siltstone.|Cross-bedded orthoquartzite with siltstone horizons.|
5422|Detention Sub Group|34701|6|Mentioned|p364|||||||||
5421|Detention Sub Group quartzite|34701|6|Mentioned|p364|||||||||
5423|Detention Sub-Group|30877|4|Described|p10|||See also p13,20-21. Unit of Rocky Cape Group.||||||11-APR-07
5423|Detention Sub-Group|42358|5|Briefly described|p19|||Misspelling of Detention Subgroup?||||||
5424|Detention Sub-group|35288|6|Mentioned|Fig.2|||||||||
5447|Dial Group|31475|6|Mentioned|p81|||||||||
5447|Dial Group|36337|6|Mentioned|Photo 2|||Located between p42 and 43.||||||12-APR-07
5447|Dial Group|36788|6|Mentioned|p27|||||||||
5447|Dial Group|41994|5|Briefly described|p6|||||||||
5447|Dial Group|44105|4|Described|p192|||Includes Gnomon Mudstone, Duncan Conglomerate, Moina Sandstone.||||||12-APR-07
5447|Dial Group|63170|5|Briefly described|p192|||Includes Gnomon Mudstone.||||||07-FEB-11
5448|Dial Range Conglomerate|36788|6|Mentioned|p60|||||||||
5462|Diddleum Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Diddleum Granodiorite [M.McClenaghan Jan95]||||||
5462|Diddleum Granite|61216|5|Briefly described|p20 Fig. 7a|Early Devonian|Early Devonian|Presented as Diddleum only, in map of granites. Age: 390.4+/-2.2Ma. Part of the Scottsdale Batholith. I-type granite. Also referred to as the Diddleum Pluton.||||||10-FEB-11
5462|Diddleum Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Diddleum Suite, Scottsdale Batholith.  I-type granite, mafic, unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
5462|Diddleum Granite|69876|5|Briefly described|p304, p306 Tb 6.1, p308, p313|||Eastern Tasmania. Also appears as Diddleum body (p311). Geochemistry, Sr ratios.||Diddleum Suite.|||I-type. Foliated.|
5558|Dog Head Formation|42416|6|Mentioned|p195|||Misspelling of Dogs Head Formation?||||||
82895|Dogs Head Limestone|73209|5|Briefly described|p882|Late Ordovician|Late Ordovician|Mole Creek area, Tasmania.|||||Lime mudstone and dolomitic lime mudstone, with a variety of fossil fauna.|
5563|Dogs Head Member|42478|5|Briefly described|Fig.21 P19|||Misspelling/variation of Dogs Head Formation.||||||
73444|Dolcoath Formation|63168|5|Briefly described|p50|||Of the Success Creek Group; overlies the basal mixtite of the group. Thickness: 800m. Interbedded quartz sandstone and minor siltstone, pebbly sandstone and conglomerate. Spelling - Dalcoath and Dolcoath are used interchangeably!||||||
5571|Dolcoath Quartzite|33839|6|Mentioned|p569|||||||||
5572|Dolcoath granite|36349|6|Mentioned|p9|||||||||
5572|Dolcoath granite|37054|6|Mentioned|p439|||||||||
24923|Dolcoath leucogranite|37054|6|Mentioned|p439|||||||||
5589|Donaldson Group|35670|6|Mentioned|p20|||||||||
5589|Donaldson Group|63167|6|Mentioned|p20|||||||||
5629|Dora Conglomerate""|30278|6|Mentioned|p181|||Refers Bradley (1954). Redundant term.||||||16-APR-07
81724|Dove 'Group'|12179|6|Mentioned|p974|||Formerly known as Dove Schist. ||||||
5680|Dove Group|12179|5|Briefly described|p974|||Nomenclature of Jennings (1963). Re-assigned with Metamorphic Complex status by Turner (1989). Due to internally relatively consistency in composition with Howell and Fisher Groups, it was proposed in this study (Meffre et al., 2000) to be grouped as Mersey River Metamorphic Complex.||||||
5680|Dove Group|23326|5|Briefly described|974|||First mapped by Jennings (1963), together with Howell and Fisher Groups; their status was changed by Turner (1989) to metamorphic complexes. However, due to consistency in composition they have now been grouped together as the Mersey River Metamorphics||||||18-APR-07
5680|Dove Group|30888|6|Mentioned|p7|||Refers Spry(1958), Jennings(1963).||||||
5680|Dove Group|36817|6|Mentioned|p13|||||||||
5680|Dove Group|63167|5|Briefly described|p37|||Superseded Dove Schist. In places in this study the term Metamorphic Complex is substituted for Group, thus Dove Metamorphic Complex.||||||
5680|Dove Group|70025|6|Mentioned|p4-5|Tonian|Mesoproterozoic|Tyennan Zone.|||||(Meta)quartzite.|
5681|Dove River Granite|31475|6|Mentioned|Fig. 1|||See also Dove Granite. Not variation on Dover River Granite. (McClenaghan Feb95).||||||18-APR-07
5681|Dove River Granite|73369|4|Described|p295, p307-310, 320, 321, 330|||Pre-Devonian, probably late Cambrian. K-Ar dates range from 455 to 500 m.y.||||||
5682|Dove River Granites|33625|6|Mentioned|p187|||Misspelling of Dove River Granite [CEB Mar95]||||||
23557|Dover River granite|36374|3|Fully described|p57|||||||||
5727|Dryo Mudstone|34047|6|Mentioned|p84|Permian|Permian|Of the Bogan Gap Group.||||||18-APR-07
5729|Drys Mudstone|23837|6|Mentioned|p440 Fig.2|||||||||
5729|Drys Mudstone|30155|6|Mentioned|Fig.33.4|||||||||
5729|Drys Mudstone|30156|6|Mentioned|Fig.9|||Part of Bogan Gap Group.||||||18-APR-07
5729|Drys Mudstone|32627|5|Briefly described|p30|Permian|Permian|Of the Bogan Gap Group. Overlies Palmer Sandstone; overlain by Blackwood Conglomerate. Thickness: 100m. Dark grey to black massive-bedded, quartz mudstone with some sandy beds; unfossiliferous. See also table on p24.||||||07-FEB-08
5729|Drys Mudstone|34099|6|Mentioned|Fig.1|||Of the Bogan Gap Group.||||||18-APR-07
5747|Duck River Dolomite""|42358|5|Briefly described|p11|||Used 1934||||||
5801|Duncan Seam|40334|6|Mentioned|Fig.14|||||||||
5801|Duncan Seam|63172|5|Briefly described|p337|Late Triassic|Late Triassic|Within the Mount Nicholas Coal Measures at Fingal.||||||07-FEB-11
5802|Duncan seam|36941|6|Mentioned|p161|||||||||
5802|Duncan seam|40334|6|Mentioned|p54|||||||||
5802|Duncan seam|41911|6|Mentioned|p147|||||||||
5802|Duncan seam|69877|5|Briefly described|p383|Late Triassic|Late Triassic|Currently (2014) mined at the Duncan Colliery near Fingal. The only seam in the Fingal Tier-Dalmayne-Mt Nicholas district to have been extensively worked.||Unit in Upper Parmeener Supergroup.|||Typically consists of 2-3m of dull coal with minor clay and mudstone partings.|
5810|Dundas "Series"|32781|6|Mentioned|p586|||||||||
5811|Dundas Beds|34502|6|Mentioned|Fig.1|||Cambrian||||||
5811|Dundas Beds|66188|6|Mentioned|431|||||||||
31319|Dundas Breccia|45018|14|Not recorded|p40||Cambrian|||||||
31319|Dundas Breccia|73146|6|Mentioned|p14|||Schmidt (1993): its characteristic remanent magnetisation (ChRM) mentioned.||||||
5814|Dundas Group 'Lower'|41795|3|Fully described|p38|||||||||
5815|Dundas Group 'Upper'|41795|3|Fully described|p42|||||||||
74913|Dundas Group Correlates""|64395|6|Mentioned|p169|||Replaced by Mount Charter Group (Corbett 1992).||||||07-FEB-11
24936|Dundas Group shales|31832|6|Mentioned|p52|||||||||
5816|Dundas Group""|40890|6|Mentioned|p52|||||||||
5816|Dundas Group""|63238|6|Mentioned|p5, p10, p12|||Complex mixture of sandstone, siltstone, mudstone and conglomerate. See also p18. ||||||
5816|Dundas Group""|63612|6|Mentioned|p11|||Informal name.||||||07-FEB-11
73446|Dundas Group, "lower"|63168|6|Mentioned|p48|||Informal - see Dundas Group. ||||||
73445|Dundas Group, "upper"|63168|6|Mentioned|p48|||Informal - see Dundas Group. ||||||
73125|Dundas Group, Lower|44135|4|Described|p16, p17-18|Middle Cambrian|Middle Cambrian|Informal - see Dundas Group. Includes Razorback Conglomerate and Brewery Junction Formation||||||07-DEC-09
73125|Dundas Group, Lower|64395|5|Briefly described|p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Informal reference to lower part of Dundas Group. Contains "Judith Formation", Red Lead Conglomerate, Hodge Slate, Razorback Conglomerate and Lower Brewery Junction Formation.||||||07-FEB-11
73125|Dundas Group, Lower|69874|5|Briefly described|p127, p149|Middle Cambrian|Middle Cambrian||||Lower Brewery Junction Formation, Razorback Conglomerate, Hodge Slate, Red Lead Conglomerate, Judith Formation.|Coeval with Mount Read Volcanics.||
73312|Dundas Group, Lower""|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Includes: Judith Fm., Red Lead Conglom., Hodge slate, Razorback Conglom., Lower Brewery Junction Fm. ||||||
73312|Dundas Group, Lower""|70753|5|Briefly described|p183-184|Middle Cambrian|Middle Cambrian|Brown (1986), whose mapping indicated the Dundas Group consisted of two distinct successions, possibly separated by a break in sedimentation and now faulted against each other; this fault separates the Lower and Upper Brewery Junction Formations.||||Part-equivalent to Tyndall Group.||
73126|Dundas Group, Upper|44135|4|Described|p16, p19|Late Cambrian|Late Cambrian|Informal - see Dundas Group. Includes Misery Conglomerate. Correlates with Owen Group from the upper part of Brewery Junction Formation through to the base of Gordon Group.||||||07-DEC-09
73126|Dundas Group, Upper|64395|5|Briefly described|p174 Fig. 8.|||Informal reference to upper part of Dundas Group. Contains Upper Brewery Junction Formation, Fernfields Conglomerate, Comet Slate, Fernflow Conglomerate, Climie Formation and Misery Conglomerate.||||||07-FEB-11
73126|Dundas Group, Upper|69874|5|Briefly described|p127, p149|Late Cambrian|Middle Cambrian||||Includes: Misery Conglomerate, Professor Range sequence, Climie Formation, Comet Formation, Upper Brewery Junction Formation.|A correlate of Owen Group.||
73313|Dundas Group, Upper""|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Middle Cambrian|Includes: Upper Brewery Junction Fm., Ferfields Fm., Comet Fm., Climie Fm., and Misery Conglomerate. ||||||
73313|Dundas Group, Upper""|70753|6|Mentioned|p183-186|Ordovician|Middle Cambrian|Brown (1986), whose mapping indicated the Dundas Group consisted of two distinct successions, possibly separated by a break in sedimentation and now faulted against each other; this fault separates the Lower and Upper Brewery Junction Formations. Fossil (agnostoid, trilobite) species listed.||||Equivalent to Owen Group.||
73314|Dundas Group, lower|63238|6|Mentioned|p12|||Informal - see Dundas Group. ||||||
73314|Dundas Group, lower|73320|6|Mentioned|Map legend|Furongian|Cambrian Series 3|Dundas, Fossey Mountains and Dial Range Troughs. Map unit contains Western Volcano-Sedimentary sequences including Yolande River Sequence, part of lower Dundas Group, Mount Charter Group, Gog Range Greywacke; description of dominantly volcano-sedimentary sequences with some felsic to intermediate volcanic rocks; Cambrian Series 3 age fossils in places.||Mount Read Volcanics||||
73270|Dundas Group, lower""|63238|5|Briefly described|p12|||Name used informally to describe position of units which have been replaced by correlates of the "Rosebery Group".||||||
73270|Dundas Group, lower""|63240|6|Mentioned|p4|||Includes Razorback Conglomerate and lower Brewery Junction Fm. (upper section) - now redesignated as Tyndall Group, based on fossil evidence; and Hodge Slate, Red Lead Conglomerate and "Judith Formation" (lower section) redesignated to Western Volc.-Sed.||||||14-MAY-07
69920|Dundas Group, upper|61260|6|Mentioned|p424|||Informal - see Dundas Group. ||||||
69920|Dundas Group, upper|63240|6|Mentioned|p4|||Informal name.||||||
69920|Dundas Group, upper|73313|6|Mentioned|Map legend|Furongian|Furongian|Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, siliciclastic to polymict, Furongian fossils in places.||Owen Group||||
69920|Dundas Group, upper|73320|6|Mentioned|Map legend|Furongian|Furongian|Western Tasmania. Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, quartz-rich to polymict; Furongian fossils in places. Grouped in either Owen Group, Dension Group and correlates.||||||
73315|Dundas Group, upper""|63238|6|Mentioned|p13, p22|Late Cambrian||Informal - see Dundas Group. Fossils found in its topmost unit of sandstone-siltstone. Faulted contact with Gordon Group. ||||||
73447|Dundas Series|63168|6|Mentioned|p50 Tb. 3.1|||Of Carey (1947c). ||||||
73448|Dundas Slates|63168|6|Mentioned|p50 Tb. 3.1|||Of Twelvetrees and Ward (1910). ||||||
27764|Dundas Ultramafic Complex|22627|6|Mentioned|p136|||||||||
27764|Dundas Ultramafic Complex|41795|4|Described|p122|||||||||
27764|Dundas Ultramafic Complex|69874|4|Described|p100, p119 Table 4.2, p120 Fig 4.18|||See also p125-126, p132. Blissett (1962). 8km east of Zeehan. Small (~3 sq km). May be from a near-continuous ophiolite sheet 50 x 20 km. Older than Dundas Group.|514 +/- 5 Ma magmatic zircon (Black et al 1997).|||Faulted to west against Concert Schist. Faulted elsewhere against Dundas Group including Red Lead Conglomerate.|Ophiolite sheet. Ultramafics - layered pyroxenite & dunite. Altered to massive serpentinite. Strongly deformed, partly recrystallised.|
73816|Dundas complex|63169|5|Briefly described|p158|||Informal reference to an ultramafic rock association (layered pyroxenite-dunite succession) in the Dundas Trough.||||||31-OCT-07
40323|Dundras Group|23949|6|Mentioned|p1124 Fig. 1|||||||||
79487|Eaglehawk Gully Basalt|69874|5|Briefly described|p181|Early Ordovician|Early Ordovician|Occurs within siliciclastic rocks near Beaconsfield. Geochemistry briefly described.||||||
74080|Eaglehawk Gully basalt|61395|4|Described|p33, p26 Fig. 3.1|Ordovician|Ordovician|Informal reference to a basalt flow one third of the way up from the base of the Eaglehawk Gully Formation in Middle Arms Gorge - see Eaglehawk Gully Formation (Denison Group). Max. thickness: 20m. See also p30 Fig. 3.4.||Of the Eaglehawk Gully Formation (Denison Group).|||Transitional alkali-tholeiite.|13-MAY-16
74080|Eaglehawk Gully basalt|65646|6|Mentioned|p56 Fig.30.|Ordovician|Ordovician|?informal name. Peperitic/hyaloclastic unit in Eaglehawk Gully Formation.||||||09-JAN-15
5906|East conglomerate""|31472|6|Mentioned|Table 1|||||||||
40415|Eastern Ahrberg Group|24604|5|Briefly described|p907 Fig. 4|Neoproterozoic|Neoproterozoic|Informal - see the Ahrberg Group.||||||
78333|Eastern Quartz-phyric Sequence|63675|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|On east flank of the Central Volcanic Complex. Consists of quartz-feldspar-phyric lavas, intrusive porphyries and volcaniclastic sandstone, intruded by magnetite series granites.||||||
78333|Eastern Quartz-phyric Sequence|67655|5|Briefly described|p11||Middle Cambrian|Also presented as EQPS in text. Some controversy about Eastern Quartz-phyric Sequence (EQPS): Corbett (2002) considers it is a time equivalent of the Central Volcanic Complex (CVC), while Murphy et. al (2004) consider that it could be part of the Tyndall Group. See also Eastern Quartz-phyric volcanics p13.||Mount Read Volcanics|||Quartz-feldspar-phyric lavas, intrusive porphyries and volcaniclastic sandstone|28-MAY-14
73129|Eastern Quartz-phyric Sequence""|44135|5|Briefly described|p16|||Overlies the Sticht Range Beds and probably also interfingers with the "Central Volcanic Complex". See also Eastern Quartz-Phyric Sequence.||||||18-SEP-13
5922|Eastern View Coal Measures|23357|4|Described|52|Early Eocene|Late Cretaceous|||||||
5922|Eastern View Coal Measures|23372|3|Fully described|p251 Fig3,p248-259|Eocene|Albian|Contains 3 "mega-sequences". In the Bass Basin.||||||26-JUN-13
5922|Eastern View Coal Measures|23778|5|Briefly described|p660|||Name been replaced with Eastern View Group. Geological Province: Torquay Basin.||||||
5922|Eastern View Coal Measures|24369|5|Briefly described|p60|||Geological Province: Bass Basin.||||||24-FEB-05
5922|Eastern View Coal Measures|24551|6|Mentioned|p308|||||||||
5922|Eastern View Coal Measures|24562|5|Briefly described|p3 Table 1|||Geological Province: Otway Basin.||||||
5922|Eastern View Coal Measures|29881|6|Mentioned|p11|||||||||
5922|Eastern View Coal Measures|31245|4|Described|p83|||Tertiary||||||
5922|Eastern View Coal Measures|33155|5|Briefly described|p115|||||||||
5922|Eastern View Coal Measures|33320|6|Mentioned|p67|||Palynology||||||
5922|Eastern View Coal Measures|34063|6|Mentioned|p10|||Table. U.Cret.- Paleocene||||||
5922|Eastern View Coal Measures|35151|6|Mentioned|p150|||||||||
5922|Eastern View Coal Measures|35290|6|Mentioned|p26|||Refs Raggatt and Crespin 1952,1955.||||||26-JUN-13
5922|Eastern View Coal Measures|36499|6|Mentioned|p35|||Refers Raggatt & Crespin (1952, 1955).||||||
5922|Eastern View Coal Measures|37131|6|Mentioned|p364|||||||||
5922|Eastern View Coal Measures|38928|6|Mentioned|p22|||||||||
5922|Eastern View Coal Measures|39384|6|Mentioned|p352|||||||||
5922|Eastern View Coal Measures|41124|4|Described|p255|||||||||
5922|Eastern View Coal Measures|41201|5|Briefly described|p12|||||||||
5922|Eastern View Coal Measures|41552|6|Mentioned|p459|||||||||
5922|Eastern View Coal Measures|42541|5|Briefly described|p204|||||||||
5922|Eastern View Coal Measures|43489|6|Mentioned|5-7|||||||||
5922|Eastern View Coal Measures|43702|6|Mentioned|Fig.2,p398|Middle Eocene|Late Cretaceous|||||||
5922|Eastern View Coal Measures|44135|5|Briefly described|p46, p47||Cretaceous|Overlies Otway Group rocks. Geological province: Bass Basin.||||||07-DEC-09
5922|Eastern View Coal Measures|46988|4|Described|p201|||||||||
5922|Eastern View Coal Measures|47045|6|Mentioned|p197|||||||||
5922|Eastern View Coal Measures|48911|6|Mentioned|Table 1|||Chart 1. Correlated with Curdies Formation.||||||
5922|Eastern View Coal Measures|61155|5|Briefly described|p18|Middle Eocene|Paleocene|Includes fluvial sands. Age: extends back to pre-Cainozoic in Torquay and Bass Basins. Max. thickness: 800m in Torquay Basin; 3000m in Bass Basin. Geological Province: Torquay and Bass Basins. See also p3, p8.||||||03-MAR-10
5922|Eastern View Coal Measures|61182|5|Briefly described|p23|||Of Raggatt and Crespin (1952,1955). Together with Boonah Sandstone now superseded by Eastern View Formation. Geological Province: Otway Basin.||||||
5922|Eastern View Coal Measures|61553|6|Mentioned|p604.|||||||||
5922|Eastern View Coal Measures|63173|5|Briefly described|p349|||Geological Province: Bass Basin. Same unit as Eastern View Group.Term used in Fig. 9.5 (after Williamson et al 1987) and probably superseded by Eastern View Group?||||||07-FEB-11
5922|Eastern View Coal Measures|65715|5|Briefly described|p13|||Superseded name for Eastern View Formation.||||||
5922|Eastern View Coal Measures|69879|4|Described|p435-437,501|Eocene|Late Cretaceous|Coal and lacustrine shale provide the main hydrocarbon source rocks in Bass Basin. Hydrocarbon reservoirs occur in sands of Middle and Upper Eastern View Coal Measures; sealed by intraformational lacustrine shale or Demons Bluff Formation. Includes two intervals of intrusive or eruptive amygdaloidal olivine basalt. Miocene intrusives are common (descriptions and ages given).|||Includes Upper, Middle, Lower Eastern View Coal Measures.|Equivalent to Durroon and Bass Megasequences.|Coal and lacustrine shale. |
5922|Eastern View Coal Measures|70077|6|Mentioned|Regional: p5|||Torquay Sub-basin and Colac Trough. Time-equivalent to Massacre Shale, Pebble Point Formation and Pember Mudstone.||||||
5922|Eastern View Coal Measures|70942|6|Mentioned|p118, 119|||Incorporates old Boonah Sand unit.||||||17-FEB-17
79576|Eastern View Coal Measures, Lower|69879|5|Briefly described|p431|Campanian|Turonian|Fluvio-deltaic to lacustrine deposits.||Eastern View Coal Measures||?Equivalent to Durroon Megasequence.|Basal volcanics (36m of basalt) overlain by sandstone fining upwards into siltstone and shale (374m of sediments).|
79577|Eastern View Coal Measures, Middle|69879|5|Briefly described|p433, p435|Maastrichtian|Campanian|Sands form hydrocarbon reservoirs, sealed by intraformational lacustrine shale or Demons Bluff Formation.||Eastern View Coal Measures||Equivalent to Furneaux Sequence, Tilana Sequence.||
79578|Eastern View Coal Measures, Upper|69879|5|Briefly described|p433, p435|Eocene|Paleocene|Sands form hydrocarbon reservoirs, sealed by intraformational lacustrine shale or Demons Bluff Formation.||Eastern View Coal Measures||Equivalent to Narimba Sequence.||
5926|Eastern View Group|23778|3|Fully described|p660|Eocene|Paleocene|Formerly known as Eastern View Coal Measures. Overlying unit Demons Bluff Gp. Underlying unit Otway Gp. Torquay Basin.||||||
5926|Eastern View Group|24038|5|Briefly described|p439 Fig.2|Eocene||Geological Province: Torquay Basin.||||||01-JUL-08
5926|Eastern View Group|24551|5|Briefly described|p308|||||||||
5926|Eastern View Group|24562|5|Briefly described|p132|Tertiary|Late Cretaceous|Geological Province: Otway Basin.||||||
5926|Eastern View Group|32162|5|Briefly described|p57|||Refers Petroleum aspect||||||
5926|Eastern View Group|32574|6|Mentioned|p75|||||||||
5926|Eastern View Group|32893|6|Mentioned|p46|||Preferable to Eastern View C.M.||||||24-APR-07
5926|Eastern View Group|38731|6|Mentioned|p26|||[Variation on Victorian unit. CEBMar95]||||||
5926|Eastern View Group|40715|6|Mentioned|p59|||||||||
5926|Eastern View Group|41706|5|Briefly described|p145|||||||||
5926|Eastern View Group|41715|4|Described|p312|||||||||
5926|Eastern View Group|43252|5|Briefly described|p163|||||||||
5926|Eastern View Group|50154|5|Briefly described|p132|Miocene|Paleocene|||||||
5926|Eastern View Group|61553|6|Mentioned|p604.|||||||||
5926|Eastern View Group|62370|6|Mentioned|p455|||Geological Province: Torquay Basin||||||09-JUN-06
5926|Eastern View Group|63173|5|Briefly described|p342 Fig. 9.2, p349|Late Eocene|Late Cretaceous|Overlain by Demons Bluff Formation. Geological Province: Bass Basin. Same unit as Eastern View Coal Measures. Lithology of upper and lower sections discussed (p357).||||||07-FEB-11
5926|Eastern View Group|65316|4|Described|p596, p597 Fig 2|Lutetian|Danian|||||Unconformably overlies the Otway Group; overlain by the Demons Bluff Group.|Non-marine sequence of brown coal, clay and sand; coal measures at the top of the Group.|23-APR-12
5926|Eastern View Group|65715|5|Briefly described|p13|||Superseded name for Eastern View Formation. Group rank was not warranted, and therefore it has been demoted to formation rank.||||||
5926|Eastern View Group|67061|5|Briefly described|p545, p546 Fig.3, p551, p557. |Eocene|Campanian|Non-marine. Lower parts of this unit are equivalent to the Sherbrook Group (Otway Basin); upper parts are equivalent to the Wangerrip Group. Onshore coal measures and underlying mudstones and sandstones in this unit have sedimentological and stratigraphic affinities with similar facies in the Pember Mudstone and Pebble Point Formation (Otway Basin). Has a mid-Eocene (c.40-39 Ma) unconformity between it and the overlying Demons Bluff Group.||||Unconformably overlies the Otway Group. Is overlain unconformably by Demons Bluff Group.||
5926|Eastern View Group|69297|6|Mentioned|p99 fig 2.32, |||||||Overlain by the Demons Bluff Group. Overlies the Otway Group. ||
5926|Eastern View Group|69879|5|Briefly described|p501|Eocene|Paleocene|Petroleum exploration wells intersecting this unit provide the most detailed records of Paleocene to Eocene coastal vegetation (described in considerable detail).|||||Coal measures.|
5926|Eastern View Group|69881|5|Briefly described|p563|Eocene|Paleocene|Bass Basin. Hydrocarbon reservoir, sealed by Demons Bluff Formation shale.|||||Sands with reservoir petroleum, intraformational lacustrine shales.|
78334|Eastern quartz-phyric volcanics|67655|6|Mentioned|p13 Fig. 8||Middle Cambrian|See also Eastern Quartz-phyric Sequence p11 in this paper.||||||18-SEP-13
37233|Eastern"" Ahrberg Group|23990|6|Mentioned|p168 Fig.1|||Informal name.||||||
5951|Eddystone Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
5952|Eddystone Point coarse-grained biotite a|35824|6|Mentioned|Map legend|Devonian|Devonian|||||||
5957|Eden Formation|24549|4|Described|p6|Permian|Permian|Of the Ferntree Group.||||||24-APR-07
5957|Eden Formation|30156|6|Mentioned|p40|||Part of Bogan Gap Group.||||||24-APR-07
5957|Eden Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Of the Ferntree Group.  Grey-black mudstone.||||||06-FEB-08
5957|Eden Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
5957|Eden Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
5962|Eden Shale|34099|6|Mentioned|Fig.1|||Perm.||||||
5962|Eden Shale|63868|6|Mentioned|p23 Fig. 3|||||||||07-FEB-11
6046|Eldon Beds|41795|6|Mentioned|p61|||||||||
6047|Eldon Group sandstone and siltstone|37051|6|Mentioned|p353|||||||||
74379|Eldon beds|63170|5|Briefly described|p224|||Of Gould (1866b). Formally defined as Eldon Group by Gill and Banks (1950) which comprised Crotty Quartzite, Amber Slate, Keel and Florence Quartzites and Bell Shale. The top 60m of Keel Quartzite was later separated into Austral Creek Siltstone.||||||07-FEB-11
74379|Eldon beds|69875|6|Mentioned|p258|||Of Gould (1866), for rocks overlying the main carbonate succession (Gordon Group) near the mouth of Gordon River and equivalents in Eldon River. Later defined as Eldon Group by Gill and Banks (1950) from the Zeehan area.||||||
69923|Eldon group|61261|5|Briefly described|p428 Fig. 1|Devonian|Silurian|Informal name.||||||12-APR-07
69923|Eldon group|63244|5|Briefly described|p1|Devonian|Silurian|Informal name. Overlies Junee group.||||||
6052|Elephant Pass Formation|30155|6|Mentioned|p461|||||||||
70302|Elliot Bay Granite|61723|5|Briefly described|p818, p810 Tb. 1|Late Cambrian|Late Cambrian|Composite I-type granite. Intrudes a continuation of the Mount Read Volcanics at Low Rocky Point. Age: 498.8+/-3.3Ma.||||||10-JAN-08
70302|Elliot Bay Granite|63540|5|Briefly described|Map legend|Cambrian|Cambrian|I-type, felsic granite; weakly to strongly fractionated, oxidised. Name implied from map legend.||||||25-SEP-07
70302|Elliot Bay Granite|67106|6|Mentioned|p684||||498.8 +/- 3.3 Ma.||||Granite; I-type.|
70302|Elliot Bay Granite|71730|6|Mentioned|p32, p34, p36, p54, p59|||[Name only implied by table].|||||I-type granite.|
6099|Elliot Bay adamellite|33354|6|Mentioned|p186|||Min.age. Refers McDougall and Leggo (1965).||||||24-APR-07
73817|Elliot Bay granite|63169|6|Mentioned|p161|||||||||
83245|Ettrick River pegmatite|73369|5|Briefly described|p317|||Rb-Sr emplacement age on muscovite 750 m.y. Late Precambrian||||||
6351|Eugenana Beds|30280|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Upper Middle Devonian age||||||
6351|Eugenana Beds|30521|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Upper-Middle Devonian||||||
6351|Eugenana Beds|30718|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Upper-Middle Devonian||||||
6351|Eugenana Beds|30927|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Upper - Middle Devonian||||||
6351|Eugenana Beds|32093|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Upper-Middle Devonian||||||
6351|Eugenana Beds|32619|5|Briefly described|p464|||[Originally entered for Qld. CEBMar95]||||||
6351|Eugenana Beds|33839|6|Mentioned|p577|||||||||
6351|Eugenana Beds|33840|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Upper - Middle Devonian||||||
6351|Eugenana Beds|35203|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Middle to Upper Devonian||||||
6351|Eugenana Beds|35828|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Middle to Upper Devonian||||||
6351|Eugenana Beds|39892|6|Mentioned|p20|||||||||
6351|Eugenana Beds|40708|5|Briefly described|p95|||||||||
6351|Eugenana Beds|41492|6|Mentioned|Fig.10|||||||||
6351|Eugenana Beds|43547|14|Not recorded|p156-7,160-1||Givetian|||||||
6351|Eugenana Beds|44135|6|Mentioned|p24, p29|Middle Devonian|Middle Devonian|||||||07-DEC-09
6351|Eugenana Beds|69857|5|Briefly described|Map legend|Devonian|Devonian|||||Unconformably overlies Eldon Group (Wurawina Supergroup).|Terrestrial cavern fillings.|
6351|Eugenana Beds|73320|5|Briefly described|Map legend|Devonian|Devonian|Western Tasmania. Overlies angular unconformity attributed to major polyphase orogeny.|||||Terrestrial cavern fillings.|
6352|Eugewana beds|30312|6|Mentioned|p60|||Misspelling of Eugenana?||||||
83241|Eungenana Beds|73369|5|Briefly described|p323|||Spores indicate probably late Middle Devonian.||||Unconformably overlies Gordon Limestone.||
40006|Exton member|24548|6|Mentioned|p10|Tertiary|Tertiary|Informal - see Exton Member.||||||24-APR-07
6525|Farley Formation Lower|41895|6|Mentioned|p29|||||||||
6543|Farrell "slates"|37044|6|Mentioned|Fig.8|||||||||
30396|Farrell Quartzwacke|43131|6|Mentioned|Fig.9 p582||Middle Cambrian|||||||
74934|Farrell Rivulet Quartzwacke|64395|5|Briefly described|p174 Fig. 8|Middle Cambrian|Middle Cambrian|Written as Farrell Rvt. Quartzwacke in Figure 8 (from Corbett 1992).||||||07-FEB-11
6544|Farrell Slate series|36817|6|Mentioned|p31|||||||||
30224|Farrell Slates|638|5|Briefly described|p88 Fig. 4.2, p106|Late Cambrian|Middle Cambrian|||||||
30224|Farrell Slates|43131|5|Briefly described|p573, p568|||Misspelling of Farrell Slate?||||||
30224|Farrell Slates|43241|5|Briefly described|Map Legend||Cambrian|||||||
30224|Farrell Slates|43242|5|Briefly described|Map Legend||Cambrian|||||||
30224|Farrell Slates|43244|5|Briefly described|Map Legend||Cambrian|Of Tyndall Group.||||||08-MAY-07
30224|Farrell Slates|61412|5|Briefly described|p44, p47 Fig.37.|||Epiclastics and volcaniclastics, including crystal lithic tuffs. Apparently conformable with Owen Conglomerate.||||||16-MAY-17
30224|Farrell Slates|63169|6|Mentioned|p164|||Possibly overlain by Owen Conglomerate?||||||
30224|Farrell Slates|63238|6|Mentioned|p6, p21|||||||||
30224|Farrell Slates|69874|5|Briefly described|p159, p165, p185|||Tullah area. Strongly deformed. Hosts Ag-Pb veins, mined near Tullah, related to subsurface Devonian granites.||Western Volcano-Sedimentary Sequences.|||Black slate, micaceous quartzwacke, pumiceous and crystal-rich mass-flow sandstones, pebbly siliceous greywacke, several feldspar-phyric dacite lava flows, and a single andesite flow.|
30224|Farrell Slates|70274|6|Mentioned|p447|Cambrian|Cambrian|||Unit of Mount Read Volcanics.||Overlain by Tyndall Group. Underlain by Eastern Quarts-Phyric Sequence.||
30224|Farrell Slates|73313|6|Mentioned|Map legend|Furongian|Cambrian Series 3|Map unit includes Farrell Slates, Que River Shale, Radfords Creek Group, Gog Range Greywacke in part; description of dominantly sedimentary sequences, with minor volcanic and volcaniclastic units.||Mount Read Volcanics||||
6546|Farrell Slates and Breccias|36817|6|Mentioned|p31|||||||||
6547|Farrell Slates""|30031|6|Mentioned|p628|||||||||
6548|Farrell slate|41143|6|Mentioned|p277|||||||||
73805|Farrell slates|638|6|Mentioned|p89-91 Figs. 4.3 and 4.4|||Informal - see Farrell Slates. ||||||
73877|Faulkner Formation|24552|5|Briefly described|p6|||See also Faulkner Group. Non-marine sequences. Of the Lower Parmeener Supergroup. Geological Province: Tasmanian Basin.||||||07-FEB-11
6557|Faulkner Group Sandstone|41548|6|Mentioned|Fig.1|||||||||
6556|Faulkner Group Sandstone/Siltstone|38505|6|Mentioned|Fig.2|||||||||
6556|Faulkner Group Sandstone/Siltstone|38610|6|Mentioned|Fig.2|||||||||
6592|Fern Tree Formation|42320|6|Mentioned|p13|||Variation of Ferntree Mudstone||||||
6593|Fern Tree Mudstone|42320|4|Described|p10|||Misspelling of Ferntree Mudstone?[CEBMar95]||||||
6599|Fern tree Mudstone|40706|6|Mentioned|p23|||Misspelling of Ferntree Mudstone.[CEBMar95]||||||
24977|Fernfield Formation|41795|6|Mentioned|Fig.13|Late Cambrian||Misspelling of Fernfields Formation||||||
24977|Fernfield Formation|42608|6|Mentioned|p59|||Mentioned as Fernflow-Comet-Fernfield-Climie Formations||||||
30395|Fernfields Conglomerate|43131|6|Mentioned|Fig.9 p582||Late Cambrian|||||||
30395|Fernfields Conglomerate|64395|5|Briefly described|p174 Fig. 8.|Late Cambrian|Late Cambrian|Of the Dundas Group (upper part).||||||07-FEB-11
6603|Fernfields Tuff and Conglomerate|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
30394|Fernflow Conglomerate|43131|6|Mentioned|Fig.9 p582||Late Cambrian|||||||
30394|Fernflow Conglomerate|64395|5|Briefly described|p174 Fig. 8.|Late Cambrian|Late Cambrian|Of the Dundas Group (upper part).||||||07-FEB-11
6604|Fernflow Conglomerate and Tuff|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
6605|Fernflow Conglomerate""|41795|5|Briefly described|p44|||Of Elliston (1954). Thickness: 200m.||||||08-MAY-07
6609|Ferntree Formation|24552|4|Described|p5 Fig.2|Kazanian|Kazanian|See also Ferntree Mudstone. Monotonous bioturbated estuarine mudstones. Conformably overlies Malbina Formation, overlain by Cygnet Coal Measures. Geological Province: Tasmanian Basin.||||||07-FEB-11
6609|Ferntree Formation|32292|5|Briefly described|p125|||||||||
6609|Ferntree Formation|32303|6|Mentioned|p283|||||||||
6609|Ferntree Formation|33494|6|Mentioned|p49|||||||||
6609|Ferntree Formation|36799|4|Described|p19|||||||||
6609|Ferntree Formation|41855|6|Mentioned|p29|||||||||
6609|Ferntree Formation|43084|5|Briefly described|p85|||Of Lower Parmeener Supergroup.||||||08-MAY-07
6609|Ferntree Formation|43474|14|Not recorded|p7,10,11,66||Kazanian|||||||
6609|Ferntree Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Permian|Late Permian|Probably replaced by Ferntree Mudstone?||||||07-FEB-11
6609|Ferntree Formation|63263|5|Briefly described|p34, p62|Late Permian|Late Permian|Sequence characterised by a predominance of bioturbated, unfossiliferous siltstone and minor fossiliferous intervals. See also  p33 Fig. 7.||||||07-FEB-11
6609|Ferntree Formation|67543|5|Briefly described|p145 Fig.4|||Fig.4 suggests correlation with Abels Bay and Toarra Formations; with Bogan Gap, Poatina, Middle Arm and Ferntree Groups; and with Kelcey Tier Beds.|||||Poorly fossiliferous pyritic mudstone.|
6609|Ferntree Formation|69877|6|Mentioned|p372, p375|Permian|Permian|||||Overlies Abels Bay Formation. Correlated with Abels Bay and Toarra Formations. Is overlain by Cygnet Coal Measures.||
6609|Ferntree Formation|70194|6|Mentioned|p299 Fig 2, p301, p304|Guadalupian|Kungurian|Also referred to as Ferntree Group (p301).||Of Parmeener Supergroup||Overlain by Abels Bay Formation. Underlan by Minnie Pt and Malbina formations.||
6608|Ferntree Formation""|41895|6|Mentioned|p10 Fig.2|||See nomenclatural discussion on p12 on Ferntree Mudstone vs Ferntree Group etc.||||||20-FEB-08
6610|Ferntree Group""|23837|6|Mentioned|p440 Fig.2|||||||||
6610|Ferntree Group""|36788|5|Briefly described|p32|||||||||
6610|Ferntree Group""|63172|6|Mentioned|p308 Fig. 10|||Informal name.||||||07-FEB-11
6610|Ferntree Group""|63263|5|Briefly described|p33 Fig. 7|||Probably misspelt? See Ferntree Formation.||||||07-FEB-11
6612|Ferntree Mudstone Formation|36799|4|Described|p11|||||||||
75975|Ferntree Mudstone""|65645|5|Briefly described|p30 Appendix|Permian|Permian|informal? Age: Lymingtonian.||Of Lower Parmeener Supergroup.|||Glaciomarine sandstone, siltstone and mudstone.|30-MAR-12
75975|Ferntree Mudstone""|65647|6|Mentioned|Appendix p11|Roadian|Roadian|Informal or obsolete name?. Of lower Parmeener Supergroup at Mount Nassau. Approximately equivalent to Abels Bay Formation. ~180 m thick. Glaciomarine mudstone with some loadstones. Lymingtonian Stage age.||||||24-DEC-15
74129|Ferntree Mudstones and Sandstones|63820|5|Briefly described|Map legend|Permian|Permian|||||||
6613|Ferntree formation|33302|6|Mentioned|Fig.1,2|||||||||
31925|Ferntree mudstone|43876|14|Not recorded|p587||Permian|||||||
6614|Ferntree"" Group|34099|6|Mentioned|p11|||||||||
6649|Finch Creek Beds|30998|6|Mentioned|p172|||Geochronology||||||
74380|Fingal beds|63170|6|Mentioned|p235|||Part of the former 'arenite-lutite association' of Banks (1962e) together with Mathinna Slate and Quartzite and Scamander Quartzite and Slate.||||||07-FEB-11
73806|Fish Creek association""|638|6|Mentioned|p104|||Of Calver et al (1987). Correlates of the Tyndall Group. ||||||
6689|Fisher Group|12179|5|Briefly described|p974|||Nomenclature of Jennings (1963). Re-assigned with Metamorphic Complex status by Turner (1989). Due to internally relatively consistency in composition with Howell and Dove Groups, it was proposed in this study (Meffre et al., 2000) to be grouped as Mersey River Metamorphic Complex.||||||
6689|Fisher Group|23326|5|Briefly described|974|||First mapped by Jennings (1963), together with Howell and Dove Groups; their status was changed by Turner (1989) to metamorphic complexes. However, due to consistency in composition they have now been grouped together as the Mersey River Metamorphics||||||18-APR-07
6689|Fisher Group|30888|6|Mentioned|p7|||||||||
6689|Fisher Group|34416|6|Mentioned|p57|||Precambrian. Figs.1,2||||||
6689|Fisher Group|36817|6|Mentioned|p13|||||||||
6689|Fisher Group|63167|5|Briefly described|p37|Precambrian|Precambrian|In this study the term Metamorphic Complex was substituted for Group - Fisher Metamorphic Complex.||||||
6689|Fisher Group|70025|6|Mentioned|p4-5|Tonian|Mesoproterozoic|Tyennan Zone.|||||(Meta)quartzite.|
73342|Fisher Metamorphic Complex|63167|4|Described|p38|||The term Metamorphic Complex is substituted for Group (Fisher Group) in places in this study. ||||||
74649|Fitzmaurice Bay schist|64400|5|Briefly described|p2 Fig. 1b|Mesoproterozoic|Mesoproterozoic|Informal name. Age: 1238+/-46Ma.||||||07-FEB-11
6768|Florence Formation|22627|6|Mentioned|p132|||||||||
6768|Florence Formation|40070|6|Mentioned|p18|||||||||
6768|Florence Formation|41695|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
6768|Florence Formation|41795|4|Described|p64|||||||||
6768|Florence Formation|41896|6|Mentioned|p27|||Same as Florence Quartzite p28.||||||
6768|Florence Formation|63675|5|Briefly described|p15|Silurian|Silurian|Unit in Eldon Group. Shallow-marine quartz sandstone.||||||
6768|Florence Formation|67655|5|Briefly described|p16|||||Eldon Group|||Shallow-marine quartz sandstone|28-MAY-14
6768|Florence Formation|69875|6|Mentioned|p263|||See also references to Florence Quartzite [the preferred name in this chapter]: p258-263.|420-410 Ma.|||||
26557|Florence Sandstone|13996|5|Briefly described|p138|Late Silurian|Late Silurian|Frenchmans Cap area. Contains one conulariid species. See also reference to Florence Quartzite (p144).||Eldon Group.||||
26557|Florence Sandstone|29609|5|Briefly described|p3|||||||||
26557|Florence Sandstone|31852|5|Briefly described|p720|||See also p721. Ludlovian to Gedinnian.||||||08-MAY-07
26557|Florence Sandstone|33732|4|Described|p108|||||||||
26557|Florence Sandstone|33839|5|Briefly described|p576|||||||||
26557|Florence Sandstone|37727|6|Mentioned|Fig.1|||||||||
26557|Florence Sandstone|37756|6|Mentioned|p71|||||||||
26557|Florence Sandstone|40070|4|Described|p17|||||||||
26557|Florence Sandstone|41814|6|Mentioned|Map legend|Devonian||||||||
26557|Florence Sandstone|42033|6|Mentioned|p649|||||||||
26557|Florence Sandstone|42320|6|Mentioned|p10|||||||||
26557|Florence Sandstone|43244|5|Briefly described|Map Legend|Devonian|Silurian|Of the Eldon Group.||||||08-MAY-07
26557|Florence Sandstone|43245|5|Briefly described|Map Legend|Devonian|Silurian|Of Eldon Group.||||||
26557|Florence Sandstone|43249|6|Mentioned|Map Legend|Devonian|Silurian|||||||
26557|Florence Sandstone|43250|6|Mentioned|Map Legend||Devonian|Of Eldon Group. Mainly fine-grained quartz sandstone with minor interbedded siltstone and mudstone.||||||24-MAY-07
26557|Florence Sandstone|43461|14|Not recorded|p628|||Part of Eldon Group.||||||08-MAY-07
26557|Florence Sandstone|43547|14|Not recorded|Tb 152,156,158-60|||(Skalian). Part of Eldon Group.||||||08-MAY-07
26557|Florence Sandstone|63238|5|Briefly described|p14|Devonian|Devonian|||||||
26557|Florence Sandstone|69842|6|Mentioned|p10|||Dundas map; a small area of this unit, located c.1.5 km NW of Williamsford, has been reinstated (previously considered a glacial erratic).||Eldon Group.||||
26557|Florence Sandstone|70487|6|Mentioned|p10|Devonian|Devonian|Mentioned in text as comparable Tasmanian strata.|||||Sandstone.|
73249|Florence sandstone|63244|5|Briefly described|p1|Devonian|Devonian|Informal name. Of the Eldon group. Supersedes Florence Quartzite. Overlain by Bell shale. Richly fossiliferous unit.||||||08-MAY-07
6769|Florentine River Mudstone|38070|6|Mentioned|Fig.6|||p95||||||08-MAY-07
6770|Florentine Valley Beds""|31461|6|Mentioned|p47|||Refers Etheridge (1904)||||||
6770|Florentine Valley Beds""|42478|6|Mentioned|p5|||||||||
6772|Florentine Valley Mudstone|24408|6|Mentioned|p35|Ordovician|Ordovician|||||||03-MAR-05
6772|Florentine Valley Mudstone|24548|6|Mentioned|p6|Early Ordovician|Early Ordovician|Contains the brachiopod Tritoechia careyi Brown||||||
6772|Florentine Valley Mudstone|29875|6|Mentioned|p21|||||||||
6772|Florentine Valley Mudstone|30277|6|Mentioned|p211|||Refers Banks(1962).||||||
6772|Florentine Valley Mudstone|30279|6|Mentioned|p122|||Part of Junee Group (Banks 1962).||||||21-MAY-07
6772|Florentine Valley Mudstone|30598|6|Mentioned|p50|||||||||
6772|Florentine Valley Mudstone|30983|6|Mentioned|p76|||||||||
6772|Florentine Valley Mudstone|31461|4|Described|p47|||Ordovician||||||
6772|Florentine Valley Mudstone|31464|6|Mentioned|p375|||||||||
6772|Florentine Valley Mudstone|31572|6|Mentioned|p23|||Ordovician||||||
6772|Florentine Valley Mudstone|32744|6|Mentioned|p183|||Fauna. Ordovician||||||
6772|Florentine Valley Mudstone|33731|6|Mentioned|p614|||Trilobites.||||||
6772|Florentine Valley Mudstone|36047|6|Mentioned|p366|||||||||
6772|Florentine Valley Mudstone|36379|6|Mentioned|p201|||||||||
6772|Florentine Valley Mudstone|36788|6|Mentioned|p26|||||||||
6772|Florentine Valley Mudstone|39235|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
6772|Florentine Valley Mudstone|41793|6|Mentioned|p46|||||||||
6772|Florentine Valley Mudstone|42478|6|Mentioned|p5|||Superseded by Florentine Valley Formation 1974.||||||
6772|Florentine Valley Mudstone|43245|5|Briefly described|Map Legend|Early Devonian|Late Cambrian|Of Denison Group.||||||
6772|Florentine Valley Mudstone|43246|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
6772|Florentine Valley Mudstone|44135|5|Briefly described|p39|Ordovician|Ordovician|Contains fossils dated as Middle Tremadocian to Chewtonian or Early Castlemanian.||||||07-DEC-09
6772|Florentine Valley Mudstone|48846|14|Not recorded|p14,15,18,23,25|||||||||
6772|Florentine Valley Mudstone|63170|6|Mentioned|p186|||Mentioned as a lateral equivalent of Reeds Conglomerate. See also Florence Valley Formation which is most likely the correct version of the name.||||||07-FEB-11
6772|Florentine Valley Mudstone|63263|5|Briefly described|p45|Early Ordovician|Early Ordovician|Underlies Gordon Group in the Florentine Valley.||||||07-FEB-11
6772|Florentine Valley Mudstone|65652|6|Mentioned|p12|Early Ordovician|Early Ordovician|||Unit in Wurawina Supergroup.||||
6772|Florentine Valley Mudstone|69858|5|Briefly described|Map legend|Ordovician|Cambrian|||Unit in Wurawina Supergroup.||Overlies Tim Shea Sandstone. Is overlain by Gordon Group.|Shallow-marine sandstone-mudstone +/- conglomerate +/- limestone sequences; typically grey; Ordovician fossils and trace fossils in places.|
6772|Florentine Valley Mudstone|69876|5|Briefly described|p293|Early Ordovician|Early Ordovician|||||Underlies Gordon Group. Overlies Moina Sandstone.|Mudstone.|
6771|Florentine Valley Mudstone""|30277|6|Mentioned|p217|||Refers Banks(1962)||||||
74344|Flowerdale Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Early Permian|||||||07-FEB-11
74344|Flowerdale Formation|69877|5|Briefly described|p372-373|Permian|Permian|||||Overlies Bogan Gap Group, Abels Bay and Malbina Formations.|Marine deposits with fenestellid bryozoans near the base; above which is predominantly sandstone with some carbonaceous material, probably terrestrial.|
6782|Flowery Gully Limestone|23114|5|Briefly described|p468|||Underlies Grubb Shale or Grubb beds. Overlies Cabbage Tree Formation. Has sedimentological affinities with the Gordon Group.||||||
6782|Flowery Gully Limestone|23850|5|Briefly described|p790 Fig. 5|Ordovician|Ordovician|Of Gordon Group.||||||26-APR-06
6782|Flowery Gully Limestone|31195|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
6782|Flowery Gully Limestone|36047|6|Mentioned|p366|||||||||
6782|Flowery Gully Limestone|40136|5|Briefly described|p25|||||||||
6782|Flowery Gully Limestone|42877|5|Briefly described|p158|||||||||
6782|Flowery Gully Limestone|43668|4|Described|p7|Chewtonian|Lancefieldian|Of Gordon Group.||||||
6782|Flowery Gully Limestone|44135|5|Briefly described|p28|Early Ordovician|Early Ordovician|Contains Arenig conodonts near base and Lanvirn/Llandeilo conodonts near top.||||||07-DEC-09
6782|Flowery Gully Limestone|61395|4|Described|p33-34, p27 Fig. 3.2|Arenig|Arenig|Thickness: ~170m. See also  p4 Fig. 1.3, p28 Fig.3.3. Exploited for commercial lime. Mis-spelt as Flower Gully in Figs.6.5, 6.6||Of the Gordon Group||Conformably overlies Eaglehawk Gully Fm (Denison Gp); overlain by Corn Hill Beds. Correlated with Gordon Gp elsewhere in Tasmania.|Pure stylolitic deep water limestone.|17-DEC-13
6782|Flowery Gully Limestone|63170|5|Briefly described|p212|Early Ordovician|Early Ordovician|Conformable on Cabbage Tree Formation. Max. thickness: 460m.||||||07-FEB-11
6782|Flowery Gully Limestone|63251|5|Briefly described|p8, p10 Fig. 3|Ordovician|Ordovician|Of the Gordon Group. ||||||
6782|Flowery Gully Limestone|63635|5|Briefly described|p10 Fig. 4|Ordovician|Ordovician|||||||
6782|Flowery Gully Limestone|63890|4|Described|p9, p25|Ordovician|Ordovician|Comprises a lower silica zone (limestone), chert zone (limestone with lenses and patches of chert) and an upper silica zone Massive low silica limestone with a 'dolomite' bed and another mainly massive low silica limestone). Thickness: ~520m.||||||
6782|Flowery Gully Limestone|65646|5|Briefly described|p55 Fig.29, p56 Fig.30, p61.||Ordovician|Overlies Eaglehawk Gully Formation and is conformably overlain by Johnston Creek Siltstone. A correlate of Gordon Group Limestone.||||||09-JAN-15
6782|Flowery Gully Limestone|69856|5|Briefly described|Map legend|Ordovician|Ordovician|Shown as a correlate of, and included in, Gordon Group.||Unit in Gordon Group.|||Dominantly shallow-marine limestone and minor siltstone.|
6782|Flowery Gully Limestone|69874|5|Briefly described|p214|Middle Ordovician|Early Ordovician|Beaconsfield area. Fossiliferous.||||Overlies ?conformably Eaglehawk Gully Formation.||
6782|Flowery Gully Limestone|69875|4|Described|p243 Fig 5.2, p249-250, p257|Middle Ordovician|Early Ordovician|Beaconsfield district. ~460m thick. Deep-water, outer shelf deposits. Fossil control, conodonts.||Gordon Group||Unconformably underlies Johnston Creek Siltstone. Conformably overlies Cabbage Tree Formation.|Limestone, very sparsely fossiliferous, dark grey homogeneous micrite locally with chert nodules and dolomitised lenses.|
6782|Flowery Gully Limestone|69876|5|Briefly described|p342-344|Middle Ordovician|Early Ordovician|170m thick in Beaconsfield Gold Mine vicinity. Correlated with Gordon Group elsewhere in Tasmania.||Gordon Group||Overlies Eaglehawk Gully Formation (Denison Group) conformably. Underlies Johnston Creek Siltstone (Eldon Group) unconformably.|Pure stylolitic limestone of deep water origin, prone to development of karst features; caves, sinkholes common, deeply weathered clay fill derived from limestone.|
6806|Forest Conglomerate and Quartzite|22770|6|Mentioned|Fig4p770|||Probably not intended as a formal name?  Part of Togari Group?||||||08-MAY-07
6806|Forest Conglomerate and Quartzite|23191|6|Mentioned|Map Legend|||Correlates to Neoproterozoic siliceous cobble to boulder conglomerate of the Togari Group found at CQ404420.||||||
6806|Forest Conglomerate and Quartzite|42358|4|Described|p20|||||||||
6806|Forest Conglomerate and Quartzite|42552|6|Mentioned|Map legend|||||||||
6806|Forest Conglomerate and Quartzite|43587|6|Mentioned|p162|||||||||
6806|Forest Conglomerate and Quartzite|44135|4|Described|p8|Mesoproterozoic|Mesoproterozoic|Of Togari Group. Unconformable over Rocky Cape Group; under Black River Dolomite. Max.thickness: 500m? Interbedded siliceous conglom. and cross-laminated orthoquartzite; contains clasts from Rocky Cape Group quartzites. Geol. prov:Smithton Synclinorium.||||||07-DEC-09
6806|Forest Conglomerate and Quartzite|63250|5|Briefly described|p1|Neoproterozoic III|Neoproterozoic III|Basal unit of Togari Group.  Overlies Cowrie Siltstone (Rocky Cape Group). Geological Province: northeastern margin of Smithton Synclinorium. Siliceous boulder conglomerate with angular clasts of quartzite.||||||
6806|Forest Conglomerate and Quartzite|67502|4|Described|p13, p36, p43-46, p49-50, p52,p115,p167|Early Cambrian|Late Neoproterozoic|Defined at the Black River bridge (357300/5476700, AMG rel. AGD66) on the Bass Highway east of Smithton by Spry (1964). Variable in thickness (0-120 m) in this area.||Basal Togari Group.||Unconformably overlies the Cowrie Siltstone.|Open framework chert breccia interbedded with stratified pebble conglomerate and medium-grained, locally hematitic quartzarenite. Clasts mostly resemble chert of Black River Dolomite with lesser Rocky Cape Group derived clasts; quartzarenite matrix.|
6806|Forest Conglomerate and Quartzite|69849|5|Briefly described|Map legend|||Age given as Precambrian.||||Unconformably overlies Irby Siltstone (Rocky Cape Group). Is overlain by Smithton Dolomite.|Predominantly white saccharoidal quartzite and a basal quartz conglomerate.|
6806|Forest Conglomerate and Quartzite|69857|5|Briefly described|Map legend|Cambrian|Neoproterozoic|Smithton-Rocky Cape region.|||||Basal siliceous conglomerate and sandstone.|
6806|Forest Conglomerate and Quartzite|69873|6|Mentioned|p60, p63-65, p93|||Informal name, strangely persisting. See also Forest Conglomerate (p44, p60, p63-65, p82). Has total recoverable reserves of c.1 Mt of lump silica.||||||
6806|Forest Conglomerate and Quartzite|73313|6|Mentioned|Map legend|Cryogenian|Cryogenian|Map unit includes Forest Conglomerate and Quartzite, Donaldson Formation and correlates; has description of basal siliceous conglomerate and sandstone. Grouped either in Togari Group, Ahrberg Group and correlates.||||||
6806|Forest Conglomerate and Quartzite|73320|6|Mentioned|Map legend|Cryogenian|Cryogenian|Smithton - Rocky Cape region. Overlies low-angle unconformity or inferred disconformity. Map unit of basal siliceous conglomerate and sandstone includes Forest Conglomerate and Quartzite, Donaldson Formation and correlates. Grouped in either Togari Group, Ahrberg Group and correlates.||||||
6806|Forest Conglomerate and Quartzite|73331|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Map unit is a correlate of the Forest Conglomerate and Quartzite, described as monomict (with dominantly quartzite clasts) and minor polymict, massive coarse lithic breccia, and bedded lithic conglomerate with subordinate cross-laminated quartzarenite.||Togari Group||Unconformably overlies the Rocky Cape Group correlate, underlies the Black River Dolomite.||
6812|Forest Formation|42358|6|Mentioned|p21|||Misspelling of Forest Conglomerate and Quartzite?||||||
34038|Forest Quartzite|22599|5|Briefly described|p75||Neoproterozoic|In the Smithton Basin. Overlain by Black River Dolomite||||||08-MAY-07
35844|Forth Complex|23326|5|Briefly described|977, p979|||Abbreviated version of Forth Metamorphic Complex.||||||18-APR-07
83242|Forth Group|73369|5|Briefly described|p320, p321|||Precambrian. K-Ar metamorphic age ~485 m.y.||||||
6837|Forth Metamorphics|22705|6|Mentioned|Fig.2 p791|||||||||
6837|Forth Metamorphics|23019|6|Mentioned|p612, Fig.1 p610|Cambrian|Cambrian|||||||
6837|Forth Metamorphics|24604|5|Briefly described|p907 Fig. 4|Neoproterozoic|Neoproterozoic|||||||
6837|Forth Metamorphics|33348|5|Briefly described|p135|||||||||
6837|Forth Metamorphics|42891|5|Briefly described|p298, Fig.3 p300|||||||||
6837|Forth Metamorphics|61411|6|Mentioned|p3, p7.||Proterozoic|Banded garnetiferous schist and quartzite interlayered with subordinate ortho-amphibolites of tholeiitic MORB-type affinity. Metamorphosed in Early Cambrian. Unconformably overlain by Middle Cambrian volcanic/volcaniclastic units eg Isadulla Conglomerate.||||||
6837|Forth Metamorphics|61412|5|Briefly described|p6-8.||Proterozoic|Banded garnetiferous schist and quartzite interlayered with subordinate ortho-amphibolites of tholeiitic MORB-type affinity. Metamorphosed in Early Cambrian. Unconformably overlain by Middle Cambrian volcanic/volcaniclastic units eg Isadulla Conglomerate.||||||16-MAY-17
6837|Forth Metamorphics|63433|6|Mentioned|p758 Tb. 1|Early Cambrian|Early Cambrian|Informal term for Forth Metamorphic Complex. Age range: 508+/-1Ma to 523+/-2Ma; a combined age of 513+/-8Ma results.  ||||||
6837|Forth Metamorphics|68253|5|Briefly described|p1016 Fig.10|Stage 5|Stage 4|North Coast Tasmania. See also Forth Metamorphic Complex. U-Th-Pb monazite age data from Chmielowski (2009).|ca. 509 +/- 7 Ma|||||20-JUL-15
6837|Forth Metamorphics|69873|6|Mentioned|p87|||[Name superseded by Forth Metamorphic Complex. See p57].||||||
6837|Forth Metamorphics|70025|6|Mentioned|p28|||Tyennan Zone. Deformed and metamorphosed during Tyennan metamorphism.  Contains 512+\-5 Ma zircon ages (Black et al. 1997 recalculated by Foster et al. 2005) and 510+\-11 Ma monazite ages (Chmielowski 2009).||||||
6838|Forth complex|41594|6|Mentioned|p27|||||||||
6847|Fossil Bluff beds|30877|6|Mentioned|p7|||||||||
35847|Franklin "Group"|23326|6|Mentioned|974|||Of Spry (1957) - now known as Franklin Metamorphic Complex.||||||18-APR-07
35845|Franklin Complex|23326|5|Briefly described|977, p979|||Abbreviated version of Franklin Metamorphic Complex.||||||18-APR-07
6885|Franklin Group|30616|4|Described|p191|||See Map on p192.||||||09-MAY-07
6885|Franklin Group|45087|5|Briefly described|p224|||See also p225-228, 234. Chem. analyses.||||||09-MAY-07
6885|Franklin Group|63167|5|Briefly described|p41|||Term used interchangeably with Franklin Metamorphic Complex. Includes Governor River Phyllite in lower part. ||||||
6885|Franklin Group|69874|5|Briefly described|p104|||Spry (1957). Set in quotation marks in this article (absent in the original). Very similar in structural and metamorphic history to his Joyce Group. They are probably fault bounded slices of the same lithologies and are in close proximity.||Franklin Metamorphic Complex||||12-SEP-18
6885|Franklin Group|73369|5|Briefly described|p319, p332|||Precambrian schists. Eclogite dated at 500 m.y.||||||
81722|Franklin Group''|12179|5|Briefly described|p974|||Nomenclature of Spry (1957). Very similar in structural and metamorphic history to Joyce Group; fault-bounded slices of the same lithologies and are in close proximity. Superseded; see Franklin Metamorphic Complex.||||||
79148|Franklin Metamorphic Group|68314|5|Briefly described|p755 Fig.6|Middle Cambrian|Middle Cambrian|Age inferred from Fig.6.|506 +/- 8 Ma (Turner et al., 1998).||||Includes eclogite.|
34463|Franklin Metamorphics|22705|6|Mentioned|Fig.2 p791|||Informal name - probably refers to rocks of the Franklin Metamorphic Complex.||||||02-JUL-08
34463|Franklin Metamorphics|23019|6|Mentioned|p612, Fig.1 p610|Cambrian|Cambrian|||||||
6886|Franklin group|32764|6|Mentioned|p313|||||||||
6905|Freshwater Beds|30150|6|Mentioned|Fig.5|||||||||
6905|Freshwater Beds|35085|6|Mentioned|Fig.5|||||||||
6904|Freshwater Beds""|30150|6|Mentioned|p97|||||||||
6908|Freshwater Sequence Lower""|41855|6|Mentioned|p21|||||||||
6933|Furneaux Group|29585|6|Mentioned|p20|||||||||
6933|Furneaux Group|31435|6|Mentioned|p40|||||||||
6933|Furneaux Group|39927|6|Mentioned|p304|||||||||
6933|Furneaux Group|42878|6|Mentioned|p169|||||||||
6933|Furneaux Group|43045|6|Mentioned|p151|||||||||
6933|Furneaux Group|71730|6|Mentioned|p47||||||Includes the Strzelecki, Killiecrankie, Mt Kerford and Darling Range granites.|||
34992|Furneaux Island Group|23019|6|Mentioned|p610|Devonian|Devonian|Average age 315+/-40 Ma.||||||09-MAY-07
70303|Furneaux Islands Granites|61723|6|Mentioned|p816|Devonian|Devonian|Informal collective term for the granites on the Furneaux Group of islands. ||||||
7000|Garcia Formation|24549|4|Described|p6|Permian|Permian|Basal unit of  the Ferntree Group. Max Thickness: 30ft.  May be correlated with Risdon Sandstone (Hobart area)||||||09-MAY-07
7000|Garcia Formation|30156|5|Briefly described|p39|||Mainly fossil content||||||
7000|Garcia Formation|30889|6|Mentioned|p48|||Refers Green (1959). cf Garcia Sandstone at Poatina.||||||
7000|Garcia Formation|32627|6|Mentioned|p29|||Informally named in the Dabool-Weston-Garcia Formations grouping in stating that these units have "generally not been separated during mapping".||||||13-JAN-09
7000|Garcia Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|=Risdon Sandstone. Of the Ferntree Group.  Conglomeratic sandstone.||||||06-FEB-08
7000|Garcia Formation|63172|5|Briefly described|p305|||Poorly sorted sandstone conglomerate intervals. In Central Plateau area of Tasmania.||||||07-FEB-11
7000|Garcia Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
7004|Gardens Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Gardens Granodiorite.||||||
7004|Gardens Granite|61216|5|Briefly described|p20 Fig. 7a, p43|Early Devonian|Early Devonian|See also Gardens Granodiorite. Presented as Gardens only, in map of granites. Age: 399.9+/-1.5Ma. Part of the Blue Tier Batholith. I-type granite.||||||10-FEB-11
7004|Gardens Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith. I-type granite, mafic, unfractionated, reduced. Name implied from map legend.||||||
77659|Gardens Pluton|67804|5|Briefly described|p69|Middle Devonian|Early Devonian|[The word Pluton is being used as a synonym for the Granite]|400 - 391 Ma.|||Intrudes Mathinna Supergroup.|Foliated, I-type granite.|
7006|Gardens granodiorite|37797|6|Mentioned|p141|||||||||
7006|Gardens granodiorite|39927|6|Mentioned|p305|||||||||
7006|Gardens granodiorite|65646|6|Mentioned|p39.|||I-type. Euhedral to anhedral amphibole and biotite, plagioclase and intergranular K-felsdspar and quartz.||||||09-JAN-15
79491|Garfield andesite|69874|5|Briefly described|p160|Middle Cambrian|Middle Cambrian|Mount Darwin area. (Halley et a.l 1996, Duncan 1997).||Western Volcano-Sedimentary Sequences.|||Feldspar-hornblende-phyric intrusive body, mineralised and altered in part.|
7112|Geltwood Beach Formation|22686|6|Mentioned|p747|||Type section in Geltwood Beach-1 has since been reassigned to the Eumeralla Formation (Morton 1990).||||||
7112|Geltwood Beach Formation|24551|6|Mentioned|p245|||||||||
7112|Geltwood Beach Formation|29856|6|Mentioned|p37|||||||||
7112|Geltwood Beach Formation|30905|6|Mentioned|Table 7.4|||||||||
7112|Geltwood Beach Formation|33940|6|Mentioned|p400|||Lower Cretaceous.||||||09-MAY-07
7112|Geltwood Beach Formation|35013|5|Briefly described|p390|||||||||
7112|Geltwood Beach Formation|41185|6|Mentioned|Fig.4|||||||||
7112|Geltwood Beach Formation|41269|5|Briefly described|p245|||Mention Fig.2||||||
7112|Geltwood Beach Formation|41642|6|Mentioned|Table 7.4|||||||||
7112|Geltwood Beach Formation|41704|6|Mentioned|Fig.3|||||||||
7112|Geltwood Beach Formation|41769|6|Mentioned|p57|||||||||
7112|Geltwood Beach Formation|41868|4|Described|p532|||Formerly Geltwood Beach Member.||||||09-MAY-07
7112|Geltwood Beach Formation|42152|6|Mentioned|Fig.2 P4|||||||||
7112|Geltwood Beach Formation|42361|5|Briefly described|p4|||Name should be discarded. Pollen correlation with Eumeralla Formation but described as time correlation of Pretty Hill Formation.||||||09-MAY-07
7112|Geltwood Beach Formation|42524|5|Briefly described|Fig.3 P27|||||||||
7112|Geltwood Beach Formation|42555|5|Briefly described|Fig.2 P285|||||||||
7112|Geltwood Beach Formation|42827|5|Briefly described|Table 7.4|||Of Otway Group.||||||09-MAY-07
7112|Geltwood Beach Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
7112|Geltwood Beach Formation|48911|3|Fully described|p12|||L. Cret.||||||
7112|Geltwood Beach Formation|48977|6|Mentioned|Fig.5|||||||||
7112|Geltwood Beach Formation|61182|5|Briefly described|p12|||Of Reynolds et al (1968a,b). Garnet-bearing sandstone, and mudstone, interbedded with Eumeralla Formation - palynologically correlated with Eumeralla Fm - therefore name should not be used for strata in Geltwood Beach-1. Underlies Eumeralla Formation.||||||
7112|Geltwood Beach Formation|61626|5|Briefly described|p486 Fig. 2|Early Cretaceous|Early Cretaceous|Of Otway Group. Geological Province: Otway Basin.||||||07-APR-09
7112|Geltwood Beach Formation|63124|5|Briefly described|p48 Fig. 5.1|||Superseded the Geltwood Beach Member. Recommended that name should be dropped from use - see also "Geltwood Beach Formation". Geological Province: Otway Basin.||||||
7128|George River Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on George River Granodiorite.||||||
7128|George River Granite|61216|5|Briefly described|p20 Fig. 7a|||Presented as George River only, in map of granites.||||||10-FEB-11
7128|George River Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith. I-type granite, mafic to felsic, unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
7128|George River Granite|66575|6|Mentioned|p936 Fig.2,|||Mafic, unfractionated, I-type hornblende-biotite granodiorite.||||||
7128|George River Granite|71730|6|Mentioned|p33, p35, p37, p56|||[Formal name intended].|||||I-type granite.|
7130|George River granodiorite|37797|6|Mentioned|p139|||||||||
75743|German Town Tillite|66172|14|Not recorded|23|||||||||
34677|Gilbert Seamount Complex|22857|6|Mentioned|p326|||Not a formal name - structural term for seafloor microplate.||||||
34677|Gilbert Seamount Complex|22862|6|Mentioned|p326|||||||||
34677|Gilbert Seamount Complex|24570|6|Mentioned|p387|||In the Tasman Sea. Tasman Rise.||||||
70304|Gipps Creek granite|61723|6|Mentioned|p818|||Informal name for the S-type Gipps Creek phase of the Henbury Granite mass.||||||
83720|Gipps Creek suite|73514|6|Mentioned|App.4|||Ben Lomond batholith, East Tasmania Terrane. Associated with Sn-W mineralisation.|||||S-type.|
7371|Glencoe Limestone (TAS)|34099|6|Mentioned|Fig.1|||Perm.[Variation on Glencoe Formation,Tas NOT Glencoe Limestone,Vic. CEBMar95]||||||
40980|Glencoe Limestone and Shale|24547|5|Briefly described|p22-23|Permian|Permian|Informal name referring to the limestone and shale of the Glencoe Formation. Max. Thickness: 27.4m.||||||11-MAY-04
7373|Glencoe Shale|34099|6|Mentioned|Fig.1|||Permian.||||||09-MAY-07
83422|Gnomen Mudstone|69842|6|Mentioned|p7|||Ulverstone map; should be remapped: may be part of Western Volcano-sedimentary Sequence.||||||
29551|Gog Graywacke|42972|6|Mentioned|p172|||Misspelling of Gog Range Greywacke.||||||
7475|Gog Greywacke|42891|5|Briefly described|Fig.3 P300|||||||||
73279|Gog Range Greywacke""|63240|5|Briefly described|p6|||||||||14-MAY-07
73335|Gog Range greywacke|63249|5|Briefly described|p2, p8|||Informal - see Gog Range Greywacke.||||||
40732|Golden Beach formation|50111|5|Briefly described|p20|||Informal name.  Underlies the LaTrobe formation.  Geological Province: Gippsland Basin.||||||
7507|Golden Valley Formation|24547|6|Mentioned|p3 preface|||Of Wells (1957), but elevated to Group status by McKellar (1957).||||||11-APR-05
7507|Golden Valley Formation|24548|3|Fully described|p8|Permian|Permian|Overlain by Liffey Sandstone (conformable). Underlain by Quamby Mudstone (conformable). Max Thickness: 200ft. Richly fossiliferous unit. Foraminifera Calcitornella stephensi present. Basal division is massive coquina limestone, 20ft thick||||||09-MAY-07
7507|Golden Valley Formation|31461|6|Mentioned|p49|||Refers Wells (1957).||||||09-MAY-07
7508|Golden Valley Group""|30156|6|Mentioned|p39|||||||||
7508|Golden Valley Group""|34099|6|Mentioned|p30|||||||||
7508|Golden Valley Group""|35288|6|Mentioned|p54|||||||||
40007|Golden Valley Limestone and Shale|24547|5|Briefly described|p9, p21|Permian|Permian|Originally defined by Wells (1957). Superseded by Golden Valley Group.||||||11-APR-05
40007|Golden Valley Limestone and Shale|24548|5|Briefly described|p7 Fig.III|Permian|Permian|Informal name - see Golden Valley Formation. See also Map 4687||||||
7509|Golden Valley Mudstone|32290|6|Mentioned|p74|||||||||
74126|Golden Valley Mudstones and Marl|63820|5|Briefly described|Map legend|Permian|Permian|||||||
25018|Golden Valley"" Formation|30889|6|Mentioned|p47|||||||||
7510|Golden Valley"" Group|30889|6|Mentioned|p47|||||||||
7525|Gomorrah Formation|41908|6|Mentioned|p49|||Reserved as Gomorrah Dolomite.||||||09-MAY-07
40512|Gordon Group Limestone|23948|6|Mentioned|p1098|||Informal name for the limestone of the Gordon Group.||||||
40512|Gordon Group Limestone|63169|5|Briefly described|p157 Fig. 5.2, p159 Fig. 5.4|Ordovician|Ordovician|Informal name referring to limestone within the Gordon Group. Geological Province: Dundas Trough.||||||31-OCT-07
40512|Gordon Group Limestone|67104|6|Mentioned|p635|Early Ordovician|Early Ordovician|Platform succession. Correlates with the Digger Island Limestone in Victoria.||||||
69924|Gordon Group limestone|61261|6|Mentioned|p431 Fig. 4|||Informal - see Gordon Group. ||||||
69924|Gordon Group limestone|63171|6|Mentioned|p292|||Informal refernce to limestone in the Gordon Group, or to the Gordon Limestone?||||||
69924|Gordon Group limestone|63263|6|Mentioned|p22, p31|Ordovician|Ordovician|||||||07-FEB-11
69924|Gordon Group limestone|63612|5|Briefly described|p11, p14|||Informal - refers to a limestone in the Gordon Group.||||||07-FEB-11
69924|Gordon Group limestone|73489|6|Mentioned|p655|Darriwilian|Darriwilian|||Gordon Group|||Includes sandstone interbeds.|
7591|Gordon Limestone|23163|6|Mentioned|p7|||||||||
7591|Gordon Limestone|23543|4|Described|p414-415|||also see Fig 1 p410.||||||
7591|Gordon Limestone|23739|6|Mentioned|p234|||||||||
7591|Gordon Limestone|23923|5|Briefly described|p1215, 1216, 1218 Fig, 3|Early Devonian|Ordovician|Also known as the Gordon Group.  Underlying unit: Moina Sandstone.||||||
7591|Gordon Limestone|23990|5|Briefly described|p173|Ordovician|Ordovician|||||||
7591|Gordon Limestone|24547|5|Briefly described|p9|Ordovician|Ordovician|Unconformably overlain by Stockers Tillite. See also App.2.||||||11-MAY-04
7591|Gordon Limestone|24548|3|Fully described|p7|Late Ordovician|Late Ordovician|Of the Junee Group. Conformably underlain by Caroline Creek Sandstone. Max Thickness: 1000ft. See also Maps 4687 and 46-88||||||04-MAR-08
7591|Gordon Limestone|24601|5|Briefly described|p840, p840 Fig.3, p847|Ordovician|Ordovician|~300 m thick stylolitic, dark coloured limestone.||Of Gordon Group.||Overlies the Pioneer Sandstone with a gradational contact. Conformably overlain by Eldon Group.||16-MAR-12
7591|Gordon Limestone|29456|6|Mentioned|p432|||||||||
7591|Gordon Limestone|29585|6|Mentioned|p18|||||||||
7591|Gordon Limestone|29609|6|Mentioned|Fig.1|||||||||
7591|Gordon Limestone|29626|6|Mentioned|p160|||||||||
7591|Gordon Limestone|29875|6|Mentioned|p21|||||||||
7591|Gordon Limestone|30156|5|Briefly described|p35|||Refers Balme(1960).Strongly deformed. Ordovician age.||||||
7591|Gordon Limestone|30209|6|Mentioned|p14|||||||||
7591|Gordon Limestone|30211|5|Briefly described|p17|||||||||
7591|Gordon Limestone|30212|5|Briefly described|p28|||See also P30.||||||
7591|Gordon Limestone|30213|6|Mentioned|p11|||||||||
7591|Gordon Limestone|30277|6|Mentioned|p207|||Divided into three formations||||||
7591|Gordon Limestone|30278|6|Mentioned|p178|||Early to Late Ordovician age||||||
7591|Gordon Limestone|30279|6|Mentioned|p122|||Part of Junee Group(Banks,1962)||||||
7591|Gordon Limestone|30598|6|Mentioned|p50|||||||||
7591|Gordon Limestone|30887|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
7591|Gordon Limestone|30889|5|Briefly described|p27|||See also P23||||||
7591|Gordon Limestone|30983|5|Briefly described|p76|||||||||
7591|Gordon Limestone|31138|6|Mentioned|p632|||||||||
7591|Gordon Limestone|31174|4|Described|p172|||Ordovician||||||
7591|Gordon Limestone|31175|5|Briefly described|p37|||||||||
7591|Gordon Limestone|31216|6|Mentioned|p77|||Refers Etheridge (1900) & Banks (1962)||||||
7591|Gordon Limestone|31461|4|Described|p47|||Ordovician||||||
7591|Gordon Limestone|31462|6|Mentioned|p379|||Ord.-Sil. See also Fig.2||||||
7591|Gordon Limestone|31463|4|Described|p47|||Ordovician||||||
7591|Gordon Limestone|31464|6|Mentioned|p375|||Overlies Owen Congl. & Caroline Cr. Sst. throughout Tas.||||||
7591|Gordon Limestone|31467|6|Mentioned|p118|||||||||
7591|Gordon Limestone|31472|6|Mentioned|Table 1|||||||||
7591|Gordon Limestone|31648|5|Briefly described|p31|||See also P35, 37, 38 & Fig. 2. Ordovician.||||||
7591|Gordon Limestone|31871|6|Mentioned|p6|||||||||
7591|Gordon Limestone|32290|6|Mentioned|Fig. 20|||Ord.||||||
7591|Gordon Limestone|32619|6|Mentioned|p464|||Ord.||||||
7591|Gordon Limestone|32627|5|Briefly described|p22|||Described in terms of Gordon Limestone correlates. See also p23.||||||06-FEB-08
7591|Gordon Limestone|32744|6|Mentioned|p183|||Fauna. Ordovician||||||
7591|Gordon Limestone|32794|6|Mentioned|p611|||||||||
7591|Gordon Limestone|33218|6|Mentioned|Fig.2|||||||||
7591|Gordon Limestone|33435|6|Mentioned|p128|||Silurian.||||||
7591|Gordon Limestone|33731|6|Mentioned|p612|||Refers Whittington (1966).||||||
7591|Gordon Limestone|33732|6|Mentioned|p109|||Ord.||||||
7591|Gordon Limestone|33733|6|Mentioned|p473|||||||||
7591|Gordon Limestone|33735|6|Mentioned|p246|||||||||
7591|Gordon Limestone|33737|6|Mentioned|p169|||||||||
7591|Gordon Limestone|33839|4|Described|p575|||||||||
7591|Gordon Limestone|33853|6|Mentioned|Fig.1|||Ord.||||||
7591|Gordon Limestone|34012|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
7591|Gordon Limestone|34189|3|Fully described|p5|||Ordovician.||||||
7591|Gordon Limestone|34287|6|Mentioned|p71|||See also P84. May refer to obsolete unit in South Australia [CEBJun95].||||||
7591|Gordon Limestone|34298|6|Mentioned|Table 1|||Ord.||||||
7591|Gordon Limestone|34316|5|Briefly described|p21 Fig.3|Devonian|Devonian|Age is Devonian. Overlain by Golden Valley Group rocks.||||||06-FEB-08
7591|Gordon Limestone|34501|6|Mentioned|p40|||Diagram. See also PP41,42,44 etc||||||
7591|Gordon Limestone|34502|6|Mentioned|Fig.2|||Cambrian||||||
7591|Gordon Limestone|34575|6|Mentioned|p643|||See also p644||||||09-MAY-22
7591|Gordon Limestone|34576|6|Mentioned|p346|||Fauna||||||
7591|Gordon Limestone|35034|6|Mentioned|p85|||||||||
7591|Gordon Limestone|35048|4|Described|p201|||||||||
7591|Gordon Limestone|35118|6|Mentioned|p428|||||||||
7591|Gordon Limestone|35153|6|Mentioned|Fig.1|||||||||
7591|Gordon Limestone|35155|6|Mentioned|Table.1|||Reference Elliston (1954).||||||
7591|Gordon Limestone|35668|6|Mentioned|Fig.1|||||||||
7591|Gordon Limestone|35791|6|Mentioned|p226|||||||||
7591|Gordon Limestone|35818|5|Briefly described|p6|||||||||
7591|Gordon Limestone|35819|4|Described|p8|||||||||
7591|Gordon Limestone|35844|6|Mentioned|p10, Fig. 12|||Stratigraphy and fossil content.||||||24-MAY-07
7591|Gordon Limestone|36047|4|Described|p365|||||||||
7591|Gordon Limestone|36053|6|Mentioned|p435|||See also Fig.1.||||||
7591|Gordon Limestone|36161|6|Mentioned|Fig.1|||||||||
7591|Gordon Limestone|36339|5|Briefly described|p34|||||||||
7591|Gordon Limestone|36345|6|Mentioned|p16|||||||||
7591|Gordon Limestone|36349|6|Mentioned|p9|||||||||
7591|Gordon Limestone|36350|6|Mentioned|Fig.1|||||||||
7591|Gordon Limestone|36373|6|Mentioned|p37|||||||||
7591|Gordon Limestone|36534|6|Mentioned|p226|||||||||
7591|Gordon Limestone|36732|6|Mentioned|p297|||||||||
7591|Gordon Limestone|36788|3|Fully described|p27|||||||||
7591|Gordon Limestone|36817|4|Described|p46|||||||||
7591|Gordon Limestone|36957|6|Mentioned|p142|||||||||
7591|Gordon Limestone|37044|6|Mentioned|p196|||||||||
7591|Gordon Limestone|37045|6|Mentioned|p210|||||||||
7591|Gordon Limestone|37046|6|Mentioned|p232|||||||||
7591|Gordon Limestone|37047|6|Mentioned|p248|||See also Fig.1.||||||
7591|Gordon Limestone|37051|6|Mentioned|p353|||||||||
7591|Gordon Limestone|37054|5|Briefly described|p443|||||||||
7591|Gordon Limestone|37239|4|Described|p206|||||||||
7591|Gordon Limestone|38070|6|Mentioned|Fig.6|||P95||||||
7591|Gordon Limestone|38200|6|Mentioned|p79|||||||||
7591|Gordon Limestone|38786|6|Mentioned|p89|||||||||
7591|Gordon Limestone|38993|6|Mentioned|p5|||||||||
7591|Gordon Limestone|39574|6|Mentioned|p155|||||||||
7591|Gordon Limestone|39892|6|Mentioned|p14|||||||||
7591|Gordon Limestone|40070|4|Described|p17|||||||||
7591|Gordon Limestone|40071|6|Mentioned|p35|||||||||
7591|Gordon Limestone|40072|6|Mentioned|p158|||||||||
7591|Gordon Limestone|40461|6|Mentioned|p368|||||||||
7591|Gordon Limestone|40760|4|Described|p176|||||||||
7591|Gordon Limestone|40890|6|Mentioned|p53|||See also P59||||||
7591|Gordon Limestone|41606|4|Described|p65|||||||||
7591|Gordon Limestone|41697|6|Mentioned|Map legend|||||||||
7591|Gordon Limestone|41795|6|Mentioned|p45|||||||||
7591|Gordon Limestone|41814|6|Mentioned|Map legend|Ordovician||||||||
7591|Gordon Limestone|41815|6|Mentioned|Map legend|Ordovician||||||||
7591|Gordon Limestone|41896|6|Mentioned|p25|||||||||
7591|Gordon Limestone|41934|6|Mentioned|Map legend|Ordovician||||||||
7591|Gordon Limestone|41951|5|Briefly described|p83|||||||||
7591|Gordon Limestone|42107|6|Mentioned|p306|||||||||
7591|Gordon Limestone|42170|5|Briefly described|p136|||||||||
7591|Gordon Limestone|42381|6|Mentioned|p85|||Used as a collective name for limestones within the Gordon Group.||||||
7591|Gordon Limestone|42551|6|Mentioned|Map legend|||||||||
7591|Gordon Limestone|42841|6|Mentioned|p5|||Same as Gordon Limestone Formation.||||||
7591|Gordon Limestone|42877|6|Mentioned|p158|||||||||
7591|Gordon Limestone|42891|5|Briefly described|p305|||||||||
7591|Gordon Limestone|43164|6|Mentioned|22||Ordovician|||||||
7591|Gordon Limestone|43547|14|Not recorded|p160||Ordovician|||||||
7591|Gordon Limestone|44215|14|Not recorded|p361|||||||||
7591|Gordon Limestone|45118|6|Mentioned|p3|||||||||
7591|Gordon Limestone|45922|14|Not recorded|p.519|||||||||
7591|Gordon Limestone|48846|14|Not recorded|p7,21|||See also p10,12,13,14,18,19,22,23.||||||
7591|Gordon Limestone|61216|5|Briefly described|p53, p61|Ordovician|Ordovician|Hosts the Kara mine magnetite-scheelite deposit. Overlies Moina Sandstone. The limestone is impure: unit consists of sandstone intercalated with carbonates, overlain by limestone, which commonly occurs as coarse-grained, recrystallised, massive marble.||||||10-FEB-11
7591|Gordon Limestone|61411|6|Mentioned|p4 Fig.1.|||||||||
7591|Gordon Limestone|61412|6|Mentioned|p17.||Ordovician|||||||
7591|Gordon Limestone|63171|6|Mentioned|p287|||||||||
7591|Gordon Limestone|63240|6|Mentioned|p5|||Mentioned in connection with the mis-compilation of a large area of Moina Sandstone and its basal conglomerate as Gordon Limestone.||||||
7591|Gordon Limestone|63249|5|Briefly described|p3, p4 Tb. 1|Ordovician|Ordovician|Of the Gordon Group. Overlies the Moina Sandstone. Shallow marine to intra-tidal limestone.||||||25-JAN-08
7591|Gordon Limestone|63263|6|Mentioned|p17|Ordovician|Ordovician|Part of the Gordon Group. Also informally referred to as Gordon Group limestone.||||||07-FEB-11
7591|Gordon Limestone|63592|6|Mentioned|p41|||Host rock for gold mineralisation.||||||
7591|Gordon Limestone|64393|5|Briefly described|p70|Ordovician|Ordovician|Overlain by Bell Shale. Hosts Pb-Zn-Ag exhalative mineralisation.||||||27-MAY-14
7591|Gordon Limestone|64396|5|Briefly described|p208, p210 Fig. 2|Ordovician|Ordovician|See also p211, p222. ||||||
7591|Gordon Limestone|67654|6|Mentioned|p80, p86|||Occurs as a thrust juxtaposed sliver within the Mainwaring Group.||||||27-MAY-14
7591|Gordon Limestone|68822|6|Mentioned|p331|||||||Underlain by the Owen Conglomerate.||
7591|Gordon Limestone|69050|6|Mentioned|p38|Ordovician|Ordovician|||||Intruded by the Meredith Granite.||
7591|Gordon Limestone|69850|5|Briefly described|Map legend|||Has a correlate of dark grey carbonate rocks, calcareous mudstone, minor quartz sandstone and black clay weathering products in part fossiliferous, underlying the Eldon Group.||||||
7591|Gordon Limestone|69871|6|Mentioned|p6|Ordovician|Ordovician|Subsequently Gordon Group. A thick limestone sequence widespread across western Tasmania; rich in marine fossils on some levels.||||||
7591|Gordon Limestone|69872|6|Mentioned|p28 Fig.2.11|Ordovician|Ordovician|||||Overlies Owen Conglomerate.||
7591|Gordon Limestone|69875|6|Mentioned|p244|||Early name for the Ordovician limestone succession of the Western Tasmania Terrane; eg  Gould (1866); Banks (1957).||||||
7591|Gordon Limestone|69880|5|Briefly described|p523, 547|Ordovician|Ordovician|Florentine Valley. Caves with preservation sites for marsupial fossils, including extinct species and megafauna; some specimens dated. Associated with colloform sphalerite of recent supergene origin, overlying Zn-rich and S-poor zones in this unit.||||||
7591|Gordon Limestone|71540|6|Mentioned|p288 Fig.1|||Caveside area.||||||
7591|Gordon Limestone|73170|6|Mentioned|p799|||Is faulted against the Mount Read Volcanics in the Iron Blow deposit, Mount Lyell mine area.||||||
7591|Gordon Limestone|73186|6|Mentioned|p229, Fig.2|Katian|Dapingian|Western Tasmanian Terrane.|||||Shallow water limestone.|
7591|Gordon Limestone|73369|5|Briefly described|p323|Ordovician|Ordovician|||||Unconformably overlain by Eungenana Beds. Conformably overlain by Eldon Group.||
32408|Gordon Limestone Correlate|30889|5|Briefly described|p.27.|||||||||
7587|Gordon Limestone Formation|42841|5|Briefly described|p4|||Variation on Gordon Limestone.||||||
25931|Gordon Limestone Sub-Group|30277|2|Defined|p220|Late Ordovician|Early Ordovician|Lower to Upper Ordovician.||||||
25931|Gordon Limestone Sub-Group|35118|6|Mentioned|p427|||||||||
25931|Gordon Limestone Sub-Group|36047|6|Mentioned|Fig.1|||||||||
25931|Gordon Limestone Sub-Group|36122|6|Mentioned|Fig.1|||||||||
25931|Gordon Limestone Sub-Group|36379|6|Mentioned|p201|||||||||
25931|Gordon Limestone Sub-Group|39235|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25931|Gordon Limestone Sub-Group|41694|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
25931|Gordon Limestone Sub-Group|41795|3|Fully described|p61|||||||||
7588|Gordon Limestone Sub-group|30598|6|Mentioned|p50|||||||||
7588|Gordon Limestone Sub-group|39892|6|Mentioned|p29|||||||||
7589|Gordon Limestone Subgroup|23923|5|Briefly described|p1218|Early Devonian|Ordovician|See also Gordon Subgroup.||||||
7589|Gordon Limestone Subgroup|33739|6|Mentioned|p129|||||||||
7589|Gordon Limestone Subgroup|35646|6|Mentioned|p87|||||||||
7589|Gordon Limestone Subgroup|35844|6|Mentioned|Fig.|||Located in back pocket||||||
7589|Gordon Limestone Subgroup|39892|5|Briefly described|p14|||||||||
7589|Gordon Limestone Subgroup|41793|4|Described|p56|||||||||
7589|Gordon Limestone Subgroup|42478|6|Mentioned|p5|||||||||
7589|Gordon Limestone Subgroup|61216|6|Mentioned|p63|||Incorrectly named - should be either Gordon Limestone or Gordon Subgroup.||||||10-FEB-11
7590|Gordon Limestone""|30277|6|Mentioned|p220|||Refers Banks(1962)||||||
7590|Gordon Limestone""|33739|6|Mentioned|p129|||||||||
7590|Gordon Limestone""|35860|5|Briefly described|p237|||||||||
7590|Gordon Limestone""|36054|6|Mentioned|p437|||||||||
7590|Gordon Limestone""|41795|6|Mentioned|p45|||||||||
7590|Gordon Limestone""|42478|6|Mentioned|p3|||Superseded by Gordon Subgroup in 1974.||||||
74377|Gordon Limestones""|63170|6|Mentioned|p201|||Original term for the carbonates sequence which became the Gordon Subgroup (Corbett and Banks 1975) but now known as Gordon Group.||||||07-FEB-11
25022|Gordon Marble|37054|5|Briefly described|Fig.7|||||||||
7594|Gordon River Limestone|30277|6|Mentioned|p212|||Refers Hills and Carey(1949)||||||
7594|Gordon River Limestone|32892|6|Mentioned|p223|||||||||
7594|Gordon River Limestone|37727|6|Mentioned|Fig.1|||See also P30.||||||
7594|Gordon River Limestone|43470|14|Not recorded|p160||Silurian|See also Lexicon||||||
7594|Gordon River Limestone|69875|6|Mentioned|p244|||Early name for the Ordovician limestone succession of the Western Tasmania Terrane; eg  Gould (1866); Banks (1957).||||||
7592|Gordon River Limestone Series""|30277|6|Mentioned|p211|||Refers Nyd(1929).||||||
7593|Gordon River Limestone""|41795|6|Mentioned|p47|||||||||
7595|Gordon River quartzite|37468|6|Mentioned|Table II|||||||||
42040|Gordon Sub Group Carbonates|50091|6|Mentioned|p12 Fig. 4|Ordovician|Ordovician|Informal reference to carbonate rocks of the Gordon Subgroup.||||||
7598|Gordon Sub-Group|36512|6|Mentioned|p19|||||||||
7598|Gordon Sub-Group|41693|6|Mentioned|Map legend|Ordovician||||||||
7598|Gordon Sub-Group|41795|4|Described|p61|||||||||
7598|Gordon Sub-Group|41896|6|Mentioned|p26|||||||||
7598|Gordon Sub-Group|69851|5|Briefly described|Map legend|||Mentioned as a correlate to two unnamed units (slate and siltstone with impure limestone horizons; limestones with sandstone and siltstone horizons) in the map area.||||||
7597|Gordon Sub-Group Limestone|41795|5|Briefly described|p45|||||||||
7600|Gordon Sub-group|33738|6|Mentioned|Fig.3|||See also P44||||||
7600|Gordon Sub-group|40127|6|Mentioned|p10|||||||||
7600|Gordon Sub-group|40136|5|Briefly described|p26|||||||||
7599|Gordon Sub-group limestone|37406|6|Mentioned|Fig.4|||||||||
7604|Gordon Subgroup|13995|6|Mentioned|p77|||See also reference to Gordon Group (p69, p72, p74, p76, p89).|||Cashions Creek Limestone.|||
7604|Gordon Subgroup|23718|4|Described|p27|Ordovician|Ordovician|See also pages 11, 64.||||||
7604|Gordon Subgroup|23736|6|Mentioned|p19|||||||||
7604|Gordon Subgroup|23923|5|Briefly described|p1217|Early Devonian|Ordovician|See also Gordon Limestone Subgroup.||||||
7604|Gordon Subgroup|30275|6|Mentioned|p118|||||||||
7604|Gordon Subgroup|30281|5|Briefly described|p10|||||||||
7604|Gordon Subgroup|35646|6|Mentioned|p106|||||||||
7604|Gordon Subgroup|35671|6|Mentioned|p7|||Refers to description by Corbett and Banks(1974).||||||
7604|Gordon Subgroup|35853|6|Mentioned|Fig.1|||Stratigraphic column showing range of conodontophorids.||||||
7604|Gordon Subgroup|35860|5|Briefly described|p237|||||||||
7604|Gordon Subgroup|37406|5|Briefly described|p85|||||||||
7604|Gordon Subgroup|37408|6|Mentioned|Fig.3|||||||||
7604|Gordon Subgroup|37801|6|Mentioned|p113|||||||||
7604|Gordon Subgroup|39976|6|Mentioned|p101|||||||||
7604|Gordon Subgroup|40708|6|Mentioned|p95|||||||||
7604|Gordon Subgroup|41317|6|Mentioned|p173|||||||||
7604|Gordon Subgroup|41793|6|Mentioned|p46|||See also P56||||||
7604|Gordon Subgroup|42478|5|Briefly described|p3|||||||||
7604|Gordon Subgroup|50091|6|Mentioned|p408 Fig. 1|||Conodonts found.||||||
7604|Gordon Subgroup|60299|6|Mentioned|p223|||||||||
7604|Gordon Subgroup|61216|6|Mentioned|p61|||||||||10-FEB-11
7604|Gordon Subgroup|63170|5|Briefly described|p201|Early Silurian|Early Ordovician|Of Corbett and Banks (1975), but originally referred to as "Gordon Limestones" (Gould 1866). Renamed Gordon Group and Westfield beds included. Sequence of carbonate rocks with minor siliciclastics.||||||07-FEB-11
7604|Gordon Subgroup|69875|5|Briefly described|p244, p255|||Corbett and Banks (1974, 1975), who grouped three Formations of Florentine Valley limestone with an overlying sandstone unit. Upgraded to Group status by Burrett et al. (1984). Geochemistry described.|||||Dolomite is abundant in limestones of this unit.|
7601|Gordon Subgroup Limestone|37406|6|Mentioned|Table 1|||||||||
7602|Gordon Subgroup carbonate|37408|6|Mentioned|Fig.1|||||||||
7603|Gordon Subgroup limestone|30275|6|Mentioned|p114|||||||||
7605|Gordon limestone|40071|6|Mentioned|p35|||||||||
7605|Gordon limestone|42178|6|Mentioned|p225|||||||||
7605|Gordon limestone|43587|6|Mentioned|p170||Ordovician|||||||
7605|Gordon limestone|63244|5|Briefly described|p1|Ordovician|Ordovician|Informal name. Uppermost bed of the Junee group. Unconformably overlain by Crotty Quartzite.||||||
30018|Gould Formation|43072|6|Mentioned|p32|||||||||
30018|Gould Formation|63868|6|Mentioned|p17, p23 Fig. 3|||Basal triassic unit in Lake St Clair area.||||||07-FEB-11
83231|Grahams Road volcanics|73315|5|Briefly described|Map legend|Ediacaran|Ediacaran|||Grassy Group||Overlies the Shower Droplet Volcanics.|Massive, tholeiitic basalt, with minor volcaniclastic conglomerate.|
7676|Grandfather's Granite|42726|5|Briefly described|map legend|Late Devonian||Misspelling. Should be Grandfathers Granite.||||||
7683|Grange Formation|30150|6|Mentioned|Fig.5|||||||||
7683|Grange Formation|32292|6|Mentioned|p122|||Permian. See also p123.||||||16-MAY-07
7683|Grange Formation|36799|4|Described|p11|||||||||
7683|Grange Formation|38200|6|Mentioned|p82|||||||||
7683|Grange Formation|63173|6|Mentioned|p376 Fig. 9.23|||Cut by dolerite dyke.||||||07-FEB-11
7684|Grange Mudstone Formation|36799|4|Described|p11|||||||||
31932|Grange mudstone|43876|14|Not recorded|p587||Early Permian|||||||
73264|Granite Tor granite|63240|6|Mentioned|p3|||Informal name.||||||
73264|Granite Tor granite|69876|5|Briefly described|p297, p304, 306 Tb 6.1, p307|Carboniferous|Devonian|S-type granite. Equigranular and porphyritic varieties with K-feldspar and quartz phenocrysts. Multiple intrusive phases; cut by porphyritic, aplitic and microgranite dykes.|~364-354 Ma (K-Ar).|Conical Rocks Suite|||S-type. Pale grey-white, fine-coarse grained, biotite adamellite/alkali-feldspar granite, quartz, perthitic K-feldspar(white), plagioclase, magnetite, garnet, muscovite; accessory apatite, zircon, ilmenite, monazite, tourmaline, fluorite, topaz.|
31197|Granton Stage|43477|14|Not recorded|p31||Permian|Correlated with Dalwood Group in NSW Stage of Lower Marine Series. Incl: Berriedale lst. See also Lexicon.||||||16-MAY-07
7703|Grants Point Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation/misspelling of Grant Point Granite.||||||
7703|Grants Point Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith. I-type granite, felsic, weakly fractionated, reduced. Name implied from map legend.||||||
7703|Grants Point Granite|69876|5|Briefly described|p306 Tb 6.1, p319|Carboniferous|Devonian|Eastern Tasmania. Single body Suite. Age inferred.||||Transitional? boundary with George River Granodiorite. Intruded by Tebrakunna Dyke Swarm.|I-type granite with very little or no hornblende; ranges from granodiorite to adamellite.|
7703|Grants Point Granite|71730|6|Mentioned|p33, p35, p37, p43, p56||||||||I-type granite.|
7713|Grassy Adamellite|36341|6|Mentioned|p24|||||||||
7713|Grassy Adamellite|61216|4|Described|p30|||Small body in eastern King Island. Associated with Tungsten mineralisation. Porphyritic with megacrysts of K-feldspar and groundmass of quartz, K-feldspar, plagioclase, biotite and amphibole, with accessory apatite, allanite, sphene, magnetite and zircon||||||10-FEB-11
7714|Grassy Granite|42726|5|Briefly described|map legend|Late Devonian||Variation on Grassy Granodiorite, Grassy Adamellite.||||||
7714|Grassy Granite|61216|5|Briefly described|p19 Fig. 7|Carboniferous||Presented as Grassy only, in map of granites. Age: 350.8+/-1.7Ma.||||||10-FEB-11
7714|Grassy Granite|61723|5|Briefly described|p820, p810 Tb. 1|Devonian|Devonian|A relatively oxidised, magnetite-bearing, unfractionated I-type hornblende-biotite monzogranite. Age: 350.8+/-1.7Ma. On King Island. ||||||
7714|Grassy Granite|63540|5|Briefly described|Map legend||Devonian|Of Grassy Suite. One of the west  Tasmanian granites. Presented as the compound name - Grassy/Bold Head (granite).  I-type granite, mafic; unfractionated, oxidised. Name implied from map legend.||||||26-SEP-07
7714|Grassy Granite|66575|6|Mentioned|p967,|||Former name of Sandblow Granite.||||||
7714|Grassy Granite|68241|6|Mentioned|p14|||Replaced by the Sandblow Granite.||||||
7714|Grassy Granite|69841|5|Briefly described|p40|Carboniferous|Carboniferous|Name replaced here by Sandblow Granite.|||||Monzogranite.|
7714|Grassy Granite|70103|6|Mentioned|p18|||||||||
7714|Grassy Granite|71141|5|Briefly described|p127|Carboniferous|Carboniferous|Geochronology, geochemistry, mineralogy and K-feldspar Pb results are provided and discussed in detail.|351 +/- 2 Ma (U-Pb date)||||Commonly porphyritic, I-type granite.|
7715|Grassy Granodiorite|24270|6|Mentioned|p1609|||Geological Province: Lachlan Fold Belt.||||||
7715|Grassy Granodiorite|31733|5|Briefly described|p31|||Lower Carboniferous.||||||16-MAY-07
7715|Grassy Granodiorite|37044|6|Mentioned|p201|||||||||
7715|Grassy Granodiorite|37055|5|Briefly described|Fig.1|||||||||
7715|Grassy Granodiorite|44105|4|Described|p256-257, p280-281|||Of the Grassy Suite. Caused formation of scheelite deposits in a thick sequence of contact metamorphosed and metasomatised peltitic and calcareous sedimentary rock  of the Early Cambrian Grassy Group.||||||16-MAY-07
7715|Grassy Granodiorite|44135|5|Briefly described|p6|Early Carboniferous|Early Carboniferous|In eastern part of King Island. Intrusive granitic stock.||||||07-DEC-09
7715|Grassy Granodiorite|61216|6|Mentioned|Fig. 12 p34-35|Devonian|Devonian|See also Grassy Granite and Grassy adamellite.||||||10-FEB-11
7715|Grassy Granodiorite|63674|5|Briefly described|p9|Devonian|Devonian|Classified as I-type monzogranite-granodiorite; porphyritic with large pink K-feldspar phenocrysts. Intrudes Proterozoic sedimentary rocks (Grassy Group) of eastern King Island. Scheelite skarn deposits occur in the metamorphic aureole.||||||
7715|Grassy Granodiorite|64400|6|Mentioned|p8|Late Devonian|Late Devonian|Probably not related to Grassy Group units due to difference in ages. May have been superseded?||||||07-FEB-11
7715|Grassy Granodiorite|65644|6|Mentioned|p22|Early Carboniferous|Late Devonian|Scheelite deposits adjacent. See also Grassy granodiorite (p6).||||||27-MAR-12
7715|Grassy Granodiorite|69841|5|Briefly described|p40|Carboniferous|Carboniferous|Name replaced here by Sandblow Granite.|||||Monzogranite.|
7715|Grassy Granodiorite|69876|6|Mentioned|p347|||Black et al. (2010). Subsequently the Sandblow Granite.||||||
69936|Grassy Group volcanics|60904|5|Briefly described|p796|Neoproterozoic|Neoproterozoic|Informal name. On King Island (TAS). ||||||
7716|Grassy Group""|31468|6|Mentioned|p14|||||||||
70305|Grassy granite|61723|6|Mentioned|p825|||Informal - see Grassy Granite. I-type granite. ||||||
7719|Grassy granodiorite|31031|6|Mentioned|p436|||||||||
7719|Grassy granodiorite|65644|5|Briefly described|p6|Devonian|Devonian|Intrudes Proterozoic sediments on King Island. I-Type. See Grassy Granodiorite (p22).|||||Porphyritic adamellite-granodiorite, pink K-feldspar phenocrysts.|27-MAR-12
25028|Gray Formation|33702|6|Mentioned|p223|||Trilobites||||||
7725|Gray Limestone|41514|6|Mentioned|p81|||Contains the fossil Trepeilopsis australiensis.||||||21-MAY-07
7725|Gray Limestone|43050|6|Mentioned|p27|||One of the locations for the fossil Earlandia condoni Crespin 1958.||||||21-MAY-07
75744|Gray Siltstone and Sandstone|66174|14|Not recorded|?|||||||||
75745|Gray Stage|66174|14|Not recorded|?|||||||||
7733|Great Dome Sandstone Formation|41954|6|Mentioned|Table 1 P12|||||||||
7734|Great Dome sandstone|41793|6|Mentioned|p46|||||||||
7736|Great Lake dolerite|33347|6|Mentioned|p46|||Refers chem. anal.||||||
77773|Green Hills Volcanics|65653|6|Mentioned|p32 Fig.10i, p34.|Miocene|Miocene|Pillows, lava lobes, sheet lavas and megapillows. Basanites. Youngest dated basalts in Tasmania at 8.5 +/- 0.1 Ma.||||||
77773|Green Hills Volcanics|69879|5|Briefly described|p466|Miocene|Miocene|Near Stanley. Age inferred. Erupted under shallow marine conditions.|||||Basanitic pillow lavas, lava lobes, megapillows (lava tube feeders), tabular sheet lavas and minor hyaloclastite.|
76811|Grimes intrusive suite|64746|6|Mentioned|p388. |||[Formal name is Grimes Intrusive Suite]. These granites, with the highest crustal component, have Nd model ages of 1670 Ma and 1740 Ma.||||||27-FEB-13
7843|Grubb Beds|30887|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
7843|Grubb Beds|30889|6|Mentioned|p23|||Now included in Gordon Limestone correlate.||||||
7843|Grubb Beds|61395|6|Mentioned|p34, p60|||Of Green (1959). Probably misspelt - and should be Grubb beds. Corn Hill Beds (of Hills 1982) have been likened to these.||||||17-DEC-13
7843|Grubb Beds|64396|5|Briefly described|p210 Fig. 2, p211|Ordovician|Ordovician|Top unit of Ordovician sequence in the Beaconsfield mine. Shale.||||||08-DEC-08
7843|Grubb Beds|69875|5|Briefly described|p256|Silurian|Ordovician|Green (1959). Age inferred from probable correlation. Located at Beaconsfield.||||Probably correlates with Johnston Creek Siltstone.|Black graphitic shale 50m thick.|
35650|Grubb Shale|23114|5|Briefly described|p468|||Overlies Flowery Gully Limestone.||||||
40364|Grubb beds|23114|5|Briefly described|p468|Ordovician|Ordovician|Overlies Flowery Gully Limestone.||||||
40364|Grubb beds|61395|5|Briefly described|p34|||Mapped by Green (1959). Originally interpreted as a silty member within the Flowery Creek Limestone by Gee and Legge (1979). Max. thick> 30m. See also Grubb Beds.||||Overlies Flowery Creek Limestone.|A black graphitic shale.|17-DEC-13
78478|Guilfoyle Basalt|67654|6|Mentioned|p9|||See also Guilfoyle Creek Basalt used elsewhere in this paper. ||||||
78490|Haleys New Country granodiorite|66575|6|Mentioned|p936 Fig2,|||Mafic, unfractionated, I-type hornblende-biotite granodiorite. Intruded by Hogans Road Diorite. Shown in figure as Haleys New Country, with lithology implied from key.||||||
74271|Hall Formation|63171|6|Mentioned|p288 Fig. 7.22, p278|Cambrian|Cambrian|From figure courtesy of Aberfoyle Exploration Pty Ltd. Includes limestone.||||||27-MAY-11
7975|Hall's Formation|42178|6|Mentioned|Fig.3 P229|||||||||
26604|Halleys New Country Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Haleys New Country Adamellite [M.McClenaghan Jan95]||||||
7993|Halls Formation""|41795|6|Mentioned|p35|||||||||
7996|Halls formation|33218|5|Briefly described|p27|||||||||
8024|Hampshire Hills Granite|31141|6|Mentioned|p16|||||||||
8024|Hampshire Hills Granite|73369|6|Mentioned|p311|||Of Solomon (1962). Alternative name for Housetop Granite?||||||
8041|Hangingwall Quartzite|36083|6|Mentioned|p474|||||||||
73317|Hangingwall Volcaniclastics|63238|5|Briefly described|p19 Fig. 2|||Equivalent to White Spur Formation.||||||
73317|Hangingwall Volcaniclastics|69874|6|Mentioned|p150|||An alternative, informal name for White Spur Formation.||||Is overlain by Tyndall Group.||
8088|Harford Beds|30326|6|Mentioned|p45|||Reference Burns 1965.||||||
8088|Harford Beds|36418|5|Briefly described|p294|||Ages given.||||||
69661|Harford beds|44135|5|Briefly described|p47|Early Eocene|Paleocene|Overlain by Thirlstane Basalt. Thickness: 250m. Geological province: Devonport-Port Sorell Sub-basin. Carbonaceous mudstone, sandstone and minor conglomerate.||||||07-DEC-09
69661|Harford beds|61155|5|Briefly described|p19|Early Eocene|Late Paleocene|Thickness: 250m. In Central North Tasmania.||||||
69661|Harford beds|63173|5|Briefly described|p360 Tb. 9.3, p361|Early Eocene|Paleocene|Thickness: >250m. Geological Province: Devonport-Port Sorell Sub-basin. Carbonaceous claystone, fine sandstone, mudstone, lignite, minor conglomerate; lacustrine fluviatile.||||||07-FEB-11
73878|Harts Hill Formation|24552|5|Briefly described|p5 Fig.2|Artinskian|Artinskian|Overlies Hickman Formation. Geological Province: Tasmanian Basin.||||||07-FEB-11
73878|Harts Hill Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Early Permian|||||||07-FEB-11
81515|Hazard Granite|71100|6|Mentioned|p134|Frasnian|Frasnian|Occurs on western side of Freycinet Island. Yields SHRIMP zircon age of 379+\-2 Ma (Kositcin and Everard, 2013).||||||
73646|Hazards Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Freycinet Suite; part of South East Coast granites.  I-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||
73646|Hazards Granite|73514|6|Mentioned|p1, p9|Devonian|Devonian|Locally associated with placer Sn deposits. [Written as Hazards granite].||||||
8201|Hazelwood Complex|39772|6|Mentioned|p18|||Misspelling and abbreviation of Heazlewood River Complex.||||||21-JAN-08
8230|Heazelwood complex|38638|6|Mentioned|p1902|||Misspelling of Heazlewood?||||||
8231|Heazlewood Complex|37044|6|Mentioned|p195|||||||||
8231|Heazlewood Complex|37056|6|Mentioned|p500|||||||||
8231|Heazlewood Complex|41594|5|Briefly described|p54|||See also p27.||||||17-MAY-07
8231|Heazlewood Complex|43191|6|Mentioned|p46|||See also Heazlewood River Complex.||||||
8231|Heazlewood Complex|63169|5|Briefly described|p167|Cambrian|Cambrian|See also Heazlewood River complex. Ultramafic complex.||||||
8231|Heazlewood Complex|67502|6|Mentioned|p100||Early Cambrian|Ultramafic. Suggested as possible source of clasts to the Scopus Formation.||||||
8233|Heazlewood River Ultramafic Complex|41793|6|Mentioned|p101|||||||||
8233|Heazlewood River Ultramafic Complex|63168|6|Mentioned|p62, p67|||Of Brown (1986). ||||||
8233|Heazlewood River Ultramafic Complex|69874|4|Described|p110-112, p119 Table 4.2, p120 Fig 4.18|Middle Cambrian|Early Cambrian|See also p121, p123-125, p127-131, p133, p140, p145. Rubenach (1973). See also Heazlewood River Complex (p98 Fig 4.3, p100, p111 Fig 4.12, p129 Table 4.3, 127-131). Located between Waratah and Savage River, largest (50 sq km) and lithologically most diverse mafic-ultramafic complex in Tasmania. Is probably a major, low-angle thrust sheet, c.8 km thick. Appears randomly as Heazlewood River Cplx, Heazlewood River Complex, Heazlewood River UC, Heazlewood Complex, Heazlewood River UM Complex. Geochemistry detailed. Hosts small Cu-Au +/- Ag deposits. SHRIMP U-Pb zircon age of a tonalite representing last phase of igneous activity.|513.6 +/- 5 Ma (Black et al 1997).||Includes Nineteen Mile Creek Dunite.|Overlies and faulted contacts against and feeder dykes intrude Luina Group; probably major low-angle thrust sheet.|About 5km of ultramafic cumulates: layered dunite and harzburgite, layered pyroxenite, peridotite and gabbro; gabbro, tonalite; overlain by up to 3 km of boninitic and low Ti tholeiitic lavas.|
8234|Heazlewood River complex|33218|5|Briefly described|p7|||||||||
8234|Heazlewood River complex|33839|5|Briefly described|p569|||||||||
8234|Heazlewood River complex|42838|5|Briefly described|p374|||||||||
8234|Heazlewood River complex|63169|5|Briefly described|p158|||Informal name - see Heazlewood Complex. Includes layered dunite-harzburgite ultramafic associations. Geological Province: Dundas Trough.||||||26-OCT-07
34168|Heazlewood Ultramafic Complex|22627|6|Mentioned|p128|Middle Cambrian|Early Cambrian|Age: 510+/-6 Ma.||||||17-MAY-07
34168|Heazlewood Ultramafic Complex|22668|5|Briefly described|p17|||||||||
34168|Heazlewood Ultramafic Complex|23309|5|Briefly described|p25||Cambrian|Age:  510+/-6 Ma.||||||
34168|Heazlewood Ultramafic Complex|44135|5|Briefly described|p15|Early Cambrian|Early Cambrian|Age: 510+/-6Ma (U-Pb on tonalite:Turner 1993a; Black 1994)||||||07-DEC-09
34168|Heazlewood Ultramafic Complex|68314|5|Briefly described|p755||||514 +/- 5 Ma SHRIMP U-Pb zircon; Black et al. 1997||||Includes tonalite.|
34168|Heazlewood Ultramafic Complex|68822|6|Mentioned|p330||||513.6 +/- 5 Ma, SHRIMP zircon (Black et al. 1997)|||||
34459|Heazlewood tonalite|22705|5|Briefly described|Fig.2 p791|||Informal name - probably refers to a tonalite within the Heazlewood River Complex. See also Fig.18 p801. Age of unit : ?510+/-6 Ma.||||||02-JUL-08
34459|Heazlewood tonalite|70274|6|Mentioned|p450,462-463|Cambrian|Cambrian|Mafic-ultramafic complex, with U-Pb SHRIMP zircon age of 513.6 Ma.|513.6  +/-10 Ma.|||||08-AUG-19
8242|Heemskirk "Granite"|33854|6|Mentioned|p657|||||||||
8243|Heemskirk (red) Granite|42726|5|Briefly described|map legend|Late Devonian||Variation/subdivision of Heemskirk Granite Complex?||||||
8243|Heemskirk (red) Granite|44105|4|Described|p255|||Of the Housetop Suite (p259).||||||17-MAY-07
8243|Heemskirk (red) Granite|61216|4|Described|p19 Fig. 7|Late Devonian|Late Devonian|Informal. Presented as Heemskirk red only in map. Age: 359.9+/-1.9Ma. Part of Heemskirk Batholith - of which the red part occupies the upper section of intrusion and has been intruded by the white granite, which is the western and major part of the body||||||10-FEB-11
8243|Heemskirk (red) Granite|63540|5|Briefly described|Map legend||Devonian|Of Heemskirk red suite. Part of the South West Coast granites.  I-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||21-DEC-09
26609|Heemskirk (white) Granite|42726|5|Briefly described|map legend|Late Devonian||Variation/subdivision of Heemskirk Granite Complex?||||||
26609|Heemskirk (white) Granite|44105|4|Described|p255|||Of the Pieman Suite (p259).||||||17-MAY-07
26609|Heemskirk (white) Granite|61216|4|Described|p19 Fig. 7|Late Devonian|Late Devonian|Informal name.  Presented as Heemskirk white only in map of granites. Age: 360.9+/-1.9Ma. Part of the Heemskirk Batholith - of which it forms the western section, also the major part. Contains a tourmaline nodular facies at contact with the red granite||||||10-FEB-11
26609|Heemskirk (white) Granite|63540|5|Briefly described|Map legend||Devonian|Of Pieman Suite. One of the west  Tasmanian granites.  S-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||26-SEP-07
25050|Heemskirk Complex|31141|6|Mentioned|p16|||||||||
8244|Heemskirk Granite|22627|6|Mentioned|fig3p126|Early Carboniferous|Late Devonian|||||||
8244|Heemskirk Granite|23451|6|Mentioned|p534|||||||||
8244|Heemskirk Granite|24274|6|Mentioned|p1691|||||||||
8244|Heemskirk Granite|30281|5|Briefly described|p12|||||||||
8244|Heemskirk Granite|30294|6|Mentioned|p862|||||||||
8244|Heemskirk Granite|31141|6|Mentioned|p16|||||||||
8244|Heemskirk Granite|31174|4|Described|p235|||Geochemistry.||||||17-MAY-07
8244|Heemskirk Granite|31435|6|Mentioned|p51|||||||||
8244|Heemskirk Granite|31448|6|Mentioned|p38|||||||||
8244|Heemskirk Granite|33839|5|Briefly described|p578|||||||||
8244|Heemskirk Granite|33853|6|Mentioned|p7|||||||||
8244|Heemskirk Granite|34298|6|Mentioned|Table 1|||Devonian||||||
8244|Heemskirk Granite|34502|6|Mentioned|Fig.1|||Devonian||||||
8244|Heemskirk Granite|35153|6|Mentioned|p199|||||||||
8244|Heemskirk Granite|37044|6|Mentioned|p196|||||||||
8244|Heemskirk Granite|37052|6|Mentioned|p366|||||||||
8244|Heemskirk Granite|37053|6|Mentioned|Table 2|||||||||
8244|Heemskirk Granite|37501|6|Mentioned|p407|||||||||
8244|Heemskirk Granite|37633|6|Mentioned|Table 37|||||||||
8244|Heemskirk Granite|37926|6|Mentioned|p499|||||||||
8244|Heemskirk Granite|40070|6|Mentioned|p19|||||||||
8244|Heemskirk Granite|40073|6|Mentioned|Fig.16|||||||||
8244|Heemskirk Granite|40074|6|Mentioned|p178|||||||||
8244|Heemskirk Granite|40736|6|Mentioned|Fig.5|||||||||
8244|Heemskirk Granite|40760|5|Briefly described|p183|||||||||
8244|Heemskirk Granite|41336|5|Briefly described|p91|||||||||
8244|Heemskirk Granite|41896|6|Mentioned|p44|||||||||
8244|Heemskirk Granite|42154|6|Mentioned|p339|||||||||
8244|Heemskirk Granite|43021|5|Briefly described|p467|||||||||
8244|Heemskirk Granite|43547|14|Not recorded|p160|||340 m.y.||||||
8244|Heemskirk Granite|44105|4|Described|p255|||Consists of red granite intruded by a white granite.  See also separately named red and white granites - Heemskirk (red) Granite and Heemskirk (white) Granite.||||||03-APR-08
8244|Heemskirk Granite|44135|4|Described|p12, p21|Early Carboniferous|Devonian|Heemskirk-Granite Tor subsurface ridge. Age: 362-330.2Ma. Large intrusive of red and white granite phases, with a tourmaline nodular facies in white phase suggesting trapping of a fluid-rich phase.||||||07-DEC-09
8244|Heemskirk Granite|45087|5|Briefly described|p13|||Chemical analyses||||||
8244|Heemskirk Granite|61216|6|Mentioned|p17|||See also the informal Heemskirk white and Heemskirk red Granites. Contains Devonian epigenetic nickel mineralisation. Part of the Heemskirk Batholith which is composite, consisting of both red and white types.||||||10-FEB-11
8244|Heemskirk Granite|61723|5|Briefly described|p819, p810 Tb. 1|Devonian|Devonian|Fine- to coarse-grained, moderately to strongly fractionated, monzogranite to alkali-feldspar granite with hydrothermally altered feldspar. Both I-type and S-type granites. Age: 360.9+/-1.9 and 359.9+/-1.9Ma.||||||
8244|Heemskirk Granite|63170|6|Mentioned|p222|||Associated with emanating mineralised fluids.||||||07-FEB-11
8244|Heemskirk Granite|63171|6|Mentioned|p289|||||||||
8244|Heemskirk Granite|63250|6|Mentioned|p2 Fig. 1 (on map)|Early Carboniferous|Late Devonian|||||||
8244|Heemskirk Granite|63825|5|Briefly described|p9, p122-129|Devonian|Devonian|Geophysical interpretation of the granitoids is presented.||||||03-APR-08
8244|Heemskirk Granite|64393|5|Briefly described|p70, p76|Late Devonian|Late Devonian|Intruded the Oonah Formation causing Sn-Pb-Zn mineralisation (thermal aureole) in the Oonah Formation. Composite body of red and white granites. Detailed lithology included.||||||07-FEB-11
8244|Heemskirk Granite|67502|6|Mentioned|p16 Fig.1.|Early Carboniferous|Late Devonian|||||||
8244|Heemskirk Granite|69872|6|Mentioned|p19|||Mentioned as part of the Heemskirk-Pine Hill-Granite Tor Granite intrusion.||||||
8244|Heemskirk Granite|69874|5|Briefly described|p132, p139, p144, p153|Devonian|Devonian|Crops out less than 1km west of McIvor Hill Complex. Associated with Avebury Ni deposits. Appears as Heemskirk granite on p144.||||May underlie McIvor Hill Complex.||
8244|Heemskirk Granite|69876|4|Described|p295, p327, p332-333, p336-337, p351|Carboniferous|Late Devonian|See also p357, p360. Describes Heemskirk Red and Heemskirk White Granites generally together as a geographic unit. May be interchangeable for Heemskirk White Granite. Also Heemskirk biotite-monzogranite batholith, Heemskirk batholith. Located 1-2km NW of Avebury nickel deposit. Proximal to Lord Brassey mine in Heazlewood River Complex. Associated with Queen Hill-Severn-Montana Sn deposits, and magnetite-rich skarns at Tenth Lagoon and Comstock.|360 Ma.||Includes Heemskirk Red Granite and Heemskirk White Granite.|Intrudes McIvor Hill Mafic-Ultramafic Complex.|Granite, associated with Sn and base metal skarns.|
8244|Heemskirk Granite|71100|4|Described|p124-125,130,134|Famennian|Famennian|Geological province: Lachlan Orogen. Exposed over 140 km2 on the western coast, and has steep intrusive contacts with the Neoproterozoic Oonah Formation metasedimentary rocks. Part of an inferred E-trending sub-surface batholith at >2km depth extending to Granite Tor, including Pine Hill Granite in W Tasmania. Zircon ages from previous studies include estimates of 340+\-5 Ma (K-Ar mica; McDougall and Leggo, 1965), 357+\-7 Ma and 350+\-6 Ma for the white and red phases (Rb-Sr whole rock ages; Brooks and Compston, 1965), and 336+\-15 Ma (average Rb-Sr biotite-whole rock; Sawka et al., 1990). Formed after Tabberabberan Orogeny (c. 390 Ma; docking of E and W Tasmanian Terranes) and ensuing crustal delamination and lithospheric upwelling. Basaltic magmatism during post-collisional extension contributed enough heat to partially melt overlying lower-crusted Proterozoic amphibolites, and to assimilate considerable amounts of upper-crusted sedimentary rocks, and after a period of protracted stagnation, resulted in felsic metaluminous I-type and peraluminous S-type granites, ranging from 374 to 360 Ma.||||||
8244|Heemskirk Granite|71141|5|Briefly described|p124-p125, p127, p129-p130, p132-p135|Upper Devonian|Upper Devonian|Exposed over an area of 140km ^2 on the western coast of Tasmania. Associated with Sn-W mineralisation and formed in a post-collisional extensional margin. Geochronology, geochemistry, mineralogy and K-feldspar Pb results are provided and discussed in detail.|360 +/- 2 Ma (U-Pb date) 361  +/- 2 Ma (U-Pb date)|||Intrudes the Oonah Formation.|Moderately to strongly fractionated granite. Seperated into a 'red' fine to coarse-grained, equigranular and locally porphyritic I-type granite and an fine- to coarse-grained, equigranular, locally porphyritic S-type 'white' granite.|
8244|Heemskirk Granite|71249|6|Mentioned|p8, p15 Fig 4.6|||||||||
8244|Heemskirk Granite|73369|4|Described|p296, 311, 312, 316, 330|||K-Ar radiometric age 340+/-5 m.y. Minimum age for emplacement.|||||Adamellite.|
27797|Heemskirk Granite Complex|31141|3|Fully described|p8|||See also p9-16.||||||17-MAY-07
70307|Heemskirk Red|61723|6|Mentioned|p822 Fig. 7|||Informal reference to the red I-type phase of Heemskirk Granite.||||||
70308|Heemskirk White|61723|6|Mentioned|p822 Fig. 7|||Informal reference to the white S-type phase of Heemskirk Granite.||||||
8245|Heemskirk granite|31577|6|Mentioned|p80|||L.Carb. 350 m.y.||||||
8245|Heemskirk granite|31767|6|Mentioned|p113|||||||||
8245|Heemskirk granite|33854|6|Mentioned|p658|||||||||
8245|Heemskirk granite|37797|6|Mentioned|p148|||||||||
8245|Heemskirk granite|42178|6|Mentioned|p232|||||||||
70306|Heemskirk granites|61723|6|Mentioned|p818|||Refers to the red and white granites of Heemskirk  Granite - informal name. ||||||
8246|Heemskirk red granite|37053|6|Mentioned|Table 2|||||||||
78335|Heemskirk white granite|63675|5|Briefly described|p20|Devonian|Middle Devonian|[Informal version of Heemskirk White Granite]. Reduced white granite, strongly fractionated. Associated with the Avebury nickel deposit.||||||
78335|Heemskirk white granite|67655|6|Mentioned|p20|Devonian|Devonian|Hosts Avebury nickel deposit||||||28-MAY-14
30402|Hellyer basalt|23899|6|Mentioned|p1514|||Maximum Thickness: 220m. Informal name.||||||
30402|Hellyer basalt|23940|6|Mentioned|p916, Fig. 2|||Of the Que-Hellyer Volcanics.||||||
30402|Hellyer basalt|23944|5|Briefly described|p1008|||Informa l -see Hellyer Basalt.  Forms the uppermost unit of the Que-Hellyer Volcanics.||||||17-MAY-07
30402|Hellyer basalt|43135|5|Briefly described|p653|||Informal subdivision within Que-Hellyer Volcanics.||||||17-MAY-07
30402|Hellyer basalt|69857|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Mount Read Volcanics.|||Basaltic volcanics and minor intrusives.|
30402|Hellyer basalt|70274|5|Briefly described|p465|Cambrian|Cambrian|Intrusive emplacement into unconsolidated mudstone of the Que River Shale (Waters and Wallace, 1992, Tomes, 2011).||||||
40505|Hellyer volcanics|23945|6|Mentioned|p1039|||Not intended as a formal name.||||||
8270|Hellyerian Stage|30150|2|Defined|p93|Late Carboniferous|Late Carboniferous|||||||
8270|Hellyerian Stage|38906|4|Described|p13|||||||||
8270|Hellyerian Stage|38908|6|Mentioned|p6|||||||||
8276|Henrys basic volcanics|33218|5|Briefly described|p29|||||||||
40214|Heytesbury group|24200|5|Briefly described|p408||Late Oligocene|Informal - see Heytesbury Group. Geological Province: Otway basin.||||||
40214|Heytesbury group|24551|6|Mentioned|p248 Fig. 9.11|||||||||
40214|Heytesbury group|24562|5|Briefly described|p7|||Geological Province: Otway Basin.||||||
40214|Heytesbury group|63740|6|Mentioned|p88|Tertiary|Tertiary|||||||07-FEB-11
73319|Higgins Creek Sequence|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Late Cambrian|Probably an informal name - refers to upper part of "Rosebery Group" in the Rosebery-White Spur area. Overlain by Professor Range Sequence.||||||
8347|Hill Formation""|41795|6|Mentioned|p64|||Informally refers to Taylor's Hill Shale (1954) - mapped between Keel and Florence Formations, but later defined in the Zeehan area as Austral Creel Formation (Gill and Banks 1950)||||||17-MAY-07
8348|Hill Shale|41795|6|Mentioned|p64|||Mapped by Taylor (1954) between Keel and Florence Formations, but later defined in the Zeehan area as Austral Creel Formation (Gill and Banks 1950)||||||17-MAY-07
8400|Hodge Slate|31464|6|Mentioned|Fig.2|||Correlation chart||||||
8400|Hodge Slate|32744|5|Briefly described|p173|||Cambrian fauna||||||
8400|Hodge Slate|35791|6|Mentioned|Fig.2|||Middle and& Late Cambrian correlation chart for Tas. See also p224.||||||17-MAY-07
8400|Hodge Slate|36817|6|Mentioned|p122|||||||||
8400|Hodge Slate|40890|6|Mentioned|p53|||||||||
8400|Hodge Slate|41814|6|Mentioned|Map legend|Cambrian||||||||
8400|Hodge Slate|43131|6|Mentioned|Fig.9,p582|||||||||
8400|Hodge Slate|48846|14|Not recorded|p10,11|||||||||
8400|Hodge Slate|63169|5|Briefly described|p179|||Of the Dundas Group. Conformably overlies Red Lead Conglomerate; overlain by Razorback Conglomerate. Siltstone-rich unit. ||||||
8400|Hodge Slate|63238|5|Briefly described|p12, p13|||Formerly of the lower Dundas Group. Fossils of Undillan age. ||||||
8400|Hodge Slate|63240|6|Mentioned|p4|||Formerly part of "lower Dundas Group" (lower section) - now redesignated as Western Volcano-Sedimentary Sequence.||||||14-MAY-07
8400|Hodge Slate|64395|5|Briefly described|p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Of the Dundas Group (lower part).||||||07-FEB-11
8400|Hodge Slate|66190|5|Briefly described|p469, p471 Fig.2,  p472|||Sediments at base of Dundas Group. At Melba Flats it unconformably overlies the Serpentine Hill Complex basalt. Siltsone with minor sandstone.||||||
8400|Hodge Slate|69573|6|Mentioned|p654, 659, 665-666|Cambrian|Cambrian|Deeper water, muddy, oxygentaed, outer shelf environment. Trilobite and agnostid faunas studied; a distinctive assemblage of blind and 'normal eyed' trilobites associated with purported pelagic agnostids and sessile suspension feeders.||||||
8400|Hodge Slate|69874|4|Described|p148-149, p163|Middle Cambrian|Middle Cambrian|Dundas area. Trilobite fauna of Undillan (probably P. punctuosus Zone) age.||Dundas Group||Overlies Red Lead Conglomerate. Underlies Razorback Conglomerate. Equivalent of the Que River and Rosebery Shales.|Slate with trilobites.|
8400|Hodge Slate|70274|5|Briefly described|p450|Cambrian|Cambrian|Contains Middle Cambrian (Drumian) trilobites (Jago and Bentley 2010). Underlain unconformably by Serpentine Hill mafic-ultramafic basalts.||Unit of Dundas Group.||||
8400|Hodge Slate|70753|5|Briefly described|p183-184|Middle Cambrian|Middle Cambrian|Outer shelf sediments. Fossils, including agnostoid and trilobite species, listed. Contains the first Cambrian fossils (dendroids) reported from Tasmania (Thomas and Henderson, 1945).||||Overlies Red Lead Conglomerate conformably and Serpentine Hill Complex unconformably. Is overlain conformably by Razorback Conglomerate.||
73320|Hodge slate|63238|5|Briefly described|p20 Fig. 3|||Informal - should be Hodge Slate. Of the Lower Dundas Group. ||||||
8413|Hogans Hill granite|36374|3|Fully described|p54|||||||||
8414|Hogans Road diorite|39927|6|Mentioned|p306, Fig. 1 p304|||||||||21-DEC-09
81362|Hollway andesite|70274|6|Mentioned|p463|Cambrian|Cambrian|Potentially coeval with Que-Hellyer Volcanics?||||||
73321|Horse Paddock Andesite""|63238|6|Mentioned|p8|||Informal name for intrusive rock. Prominent magnetic signature. Drilled as the "Penghana prospect". ||||||
37071|Housetop granite|23718|6|Mentioned|p75|||Informal name.||||||17-MAY-07
37071|Housetop granite|69881|5|Briefly described|p559|||40km S of Burnie. Granite aureole contains the Kara deposit, a magnetite-rich skarn with scheelite as a by-product.||||||
40350|Housetop granitoid|23923|5|Briefly described|p1215|Devonian|Devonian|Informal-see also Housetop Granite.||||||
8533|Howards Plains porphyry|39892|6|Mentioned|p21|||||||||
35839|Howell Group|12179|5|Briefly described|p974|||Nomenclature of Jennings (1963). Re-assigned with Metamorphic Complex status by Turner (1989). Due to internally relatively consistency in composition with Dove and Fisher Groups, it was proposed in this study (Meffre et al., 2000) to be grouped as Mersey River Metamorphic Complex.||||||
35839|Howell Group|23326|5|Briefly described|974|||First mapped by Jennings (1963), together with Fisher Group; their status was changed by Turner (1989) to metamorphic complexes. However, due to consistency in composition they have now been grouped together as the Mersey River Metamorphics||||||22-MAY-07
35839|Howell Group|63167|5|Briefly described|p37|||Incorporates Arm Schist (Jennings 1963). See also Howell Metamorphic Complex where the term Metamorphic Complex has been substituted for Group. ||||||
35839|Howell Group|63433|5|Briefly described|p759, p761|Early Cambrian|Early Cambrian|Part of the Mersey River Metamorphic Complex. ||||||
35839|Howell Group|69873|5|Briefly described|p49, p89|||Spry (1958), Jennings (1963).||Unit in Mersey River Metamorphic Complex.|||Platy fine-grained quartzite and quartz-muscovite-garnet-albite schist; tend to dominate in alternating units 50m or so thick.|
35839|Howell Group|69874|5|Briefly described|p102-103|||Tyennan Region. Rocks similar to Howell Group extend south into higher reaches of Forth River. Monazite dating supports Cambrian age for metamorphism.||||Faulted against Fisher Quartzite.|Garnet-bearing schist and quartzite.|
35839|Howell Group|70025|6|Mentioned|p4-5|Tonian|Mesoproterozoic|Tyennan Zone.|||||(Meta)quartzite.|
35839|Howell Group|73369|5|Briefly described|p319, p332|||Precambrian. Muscovite from quartz-mica schist dated at 450 m.y. K-Ar||||||
73362|Howell Metamorphic Complex|63167|5|Briefly described|p43|||The term Metamorphic Complex is substituted for Group in places in this study. Underlies Fisher Metamorphic Complex. Garnetiferous rocks.||||||
40417|Hoyle amphibolite|24604|5|Briefly described|p913|||Informal name. Of the eastern"" Ahrberg Group.||||||
40417|Hoyle amphibolite|69873|6|Mentioned|p57|||REE plots.||Unit in Timbs Group.||||
8564|Humboldt Slate|41793|5|Briefly described|p39|Neoproterozoic|Neoproterozoic|Abbreviated form of the name Humboldt Slate and Dolomite of Carey and Banks (1954) appears in the text (p39). Age is given as Eocambrian. Part of the Clark Group.||||||
73330|Humboldt Slate and Dolomite|41793|5|Briefly described|p39|Neoproterozoic||Of Carey and Banks (1954). Age is given as Eocambrian. Part of the Clark Group. Thickness: 540m.||||||21-MAY-07
73272|Huskisson Group""|63238|6|Mentioned|p11, p18|||Informal - see Huskisson Group. ||||||
73272|Huskisson Group""|63240|5|Briefly described|p4|||Redesignated as Tyndall Group correlates based on fossil evidence, in the Godkin Ridge-Ring River area.||||||17-MAY-07
73272|Huskisson Group""|69874|5|Briefly described|p163, p168, p215, p230|Middle Cambrian|Middle Cambrian|Taylor (1954), Brown (1986). Huskisson River area.||||Overlies Western Volcano-Sedimentary Sequences. Is equivalent to the Tyndall Group. Is overlain by Owen Group (equivalents).|Volcaniclastic-dominated sequence: conglomerates, sandstone and lithicwacke, and siltstone. Includes some very crystal-rich sandstones.|
73130|Huskisson Group, upper|44135|6|Mentioned|p18|||Informal - see Huskisson Group.||||||07-DEC-09
30501|Huskisson River Complex|43191|6|Mentioned|p46|||Variation on Huskisson River Ultramafic Complex.||||||
30501|Huskisson River Complex|63168|6|Mentioned|p71|||Also referred to as the Husskisson River Ultramafic Complex.||||||
30501|Huskisson River Complex|63169|5|Briefly described|p158|||Includes layered pyroxenite-dunite and layered dunite-harzburgite ultramafic associations. Geological Province: Dundas Trough.||||||31-OCT-07
8601|Huskisson River Group|31463|6|Mentioned|p173|||Fauna||||||
8602|Huskisson River Ultramafic Complex|41795|5|Briefly described|p118|||||||||
8602|Huskisson River Ultramafic Complex|69874|4|Described|p100, p119 Table 4.2, p120 Fig 4.18|Early Cambrian|Early Cambrian|See also p125-126, p131-132. Brown (1986). Also Huskisson River UC. Obscured by glacial outwash to south but probably extends to Colebrook Hill. Aeromagnetic data suggest continuous at depth with Wilson River Ultramafic Complex. Ophiolite sheet magmatic age.|514 +/- 5 Ma zircon (Black et al. 1997).|||Faulted against Luina Group to east; Gordon Group to west.|Ophiolite sheet. Ultramafics - layered dunite and harzburgite, layered pyroxenite and dunite.|
35383|Ida Bay Formation|23187|6|Mentioned|p239,245|||||||||
8697|Inglis Formation|42000|6|Mentioned|p62|||||||||
8697|Inglis Formation|43022|6|Mentioned|p472|||||||||
8697|Inglis Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Early Permian|||||||07-FEB-11
8697|Inglis Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
8697|Inglis Formation|67543|5|Briefly described|p142, p144, p145 Fig.4|Artinskian|Sakmarian|Fig.4 suggests correlation with Quamby and Woody Island Formations. See also Inglis Siltstone (p146 Fig.5).||||Underlain by the Wynyard Formation.|Dropstone-poor mudstone.|
8698|Inglis Sandstone|35288|6|Mentioned|Fig.2|||||||||
78549|Interview Beds|67502|6|Mentioned|p24|||Superseded. Introduced by Spry and Ford (1957), later defined (as the Interview Slate and Quartzite) along the lower Pieman River by Spry (1962, 1964) and subsequently divided into the Interview Siltstone and an underlying unit, "Quartzite of the Lagoon River", by Gee et al. (1969).||||||
8744|Interview River Granite|42726|5|Briefly described|map legend|Late Devonian||Misspelling of Interview Granite [M.McClenaghan Jan95].||||||22-MAY-07
8744|Interview River Granite|71100|5|Briefly described|p126,130|||In contact with Pieman Heads Granite at about, or over 1km depth below surface (Leaman and Richardson, 2003).||||||
8744|Interview River Granite|71141|6|Mentioned|p130|||Possibly connected to the Piemans Head Granite.||||||
8745|Interview Siltstone|31174|6|Mentioned|Fig. 38|||Proterozoic||||||
8745|Interview Siltstone|34188|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
8745|Interview Siltstone|63167|5|Briefly described|p5, p17|Precambrian|Precambrian|Supersedes Interview Slate and Quartzite. Principle lithologies comprise finely laminated siltstone and mudstone with thin quartzite units.||||||26-SEP-07
8745|Interview Siltstone|67502|6|Mentioned|p24|||Division of the Interview Slate and Quartzite by Gee et al. (1969); that unit was formerly the Interview Beds of Spry and Ford (1957). Probably the approximate equivalent of the Balfour Subgroup.||||Probably the approximate equivalent of the Balfour Subgroup.||
8745|Interview Siltstone|69873|6|Mentioned|p43|||Of Gee et al. (1969). Obsolete: approximate equivalent to the Balfour Subgroup (Everard et al., 2007).||||||
26631|Interview Slate|42551|5|Briefly described|Map legend|Late Precambrian||Variation on Interview Siltstone.||||||
73361|Interview Slate and Quartzite|63167|5|Briefly described|p17|Precambrian|Precambrian|Of Spry (1962b, 1964). Renamed as Interview Siltstone (Gee et al (1969). Mainly chloritic slate with thin quartzite bands in type area.||||||31-JAN-08
73361|Interview Slate and Quartzite|67502|6|Mentioned|p24|||Formerly Interview Beds (Spry and Ford, 1957). Defined along the lower Pieman River by Spry (1962, 1964) and subsequently divided into the Interview Siltstone and an underlying unit, "Quartzite of the Lagoon River", by Gee et al. (1969).||||||
78550|Irishtown Dolomite|67502|6|Mentioned|p46|||Redundant, see the Black River Dolomite. Of Nye et al. 1934.||||||
8772|Irishtown Dolomite""|42358|5|Briefly described|p11|||Used 1934. Correlated with Crimson Creek Formation, Dundas Trough 1986.||||||
77499|Isadulla Conglomerate|61411|6|Mentioned|p7.||Middle Cambrian|Conglomerate with purple mudstone clasts. ||||||
27803|Jackey Formation|23837|5|Briefly described|p441|Late Permian|Late Permian|Geological Province: Tasmania Basin.||||||
27803|Jackey Formation|24549|4|Described|p5|Permian|Permian|Max Thickness: est. 140ft. Freshwater shales with plant fragments.||||||07-FEB-08
27803|Jackey Formation|30155|6|Mentioned|p465|||||||||
27803|Jackey Formation|30819|6|Mentioned|p107|||||||||
27803|Jackey Formation|30926|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
27803|Jackey Formation|32059|6|Mentioned|Map legend|Permian|Permian|||||||
27803|Jackey Formation|32627|4|Described|p23, p31|Permian|Permian|Overlies Eden Mudstone (Bogan Gap Group). Series of beds of sandstone and shale. Thickness: 43m. See also table on p24.||||||07-FEB-08
27803|Jackey Formation|34012|6|Mentioned|Map legend|Permian|Permian|||||||
27803|Jackey Formation|34047|6|Mentioned|p84|||Perm.||||||
27803|Jackey Formation|34316|5|Briefly described|p21 Fig.3|Triassic|Late Permian|Of the Cygnet Coal Measures. Shale with abundant plant fragments.||||||06-FEB-08
27803|Jackey Formation|36207|6|Mentioned|Text Fig.2|||||||||
27803|Jackey Formation|41699|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27803|Jackey Formation|41896|6|Mentioned|p33|||||||||
27803|Jackey Formation|42244|6|Mentioned|p26|||||||||
27803|Jackey Formation|43072|6|Mentioned|p32|||||||||
27803|Jackey Formation|43088|5|Briefly described|p27|||see also Longford Basin Geology map||||||
27803|Jackey Formation|46849|6|Mentioned|p197|||||||||
27803|Jackey Formation|69773|5|Briefly described|p35|Permian|Permian|Thickness of c.15m; c.43m thick elsewhere.|||||Includes feldspathic sandstone, micaceous and sometimes carbonaceous sandstone and shale, khaki-coloured shale, massively and thinly-bedded shale; a thin, lenticular bed of pebble conglomerate.|
27803|Jackey Formation|69851|5|Briefly described|Map legend|||Mentioned as a correlate to an unnamed unit, of sandstone and mudstone beds often carbonaceous with some sandstone horizons with worm burrows, in the map area.||||||
27803|Jackey Formation|69877|6|Mentioned|p376-378|Permian|Permian|||||||
8826|Jackey Shale Formation|38908|6|Mentioned|p8|||Informal name.||||||07-FEB-08
8834|Jacobs Quartzite|34701|6|Mentioned|p364|||Misspelling of Jacob?||||||
8834|Jacobs Quartzite|42358|6|Mentioned|p14|||||||||
79494|Johnston Creek Formation|69874|5|Briefly described|p138 Fig 4.37|Silurian|Silurian|||||Correlate of Eldon Group.|Quartz sandstone, laminated siltstone and shale.|
9021|Jones Creek shale|37045|6|Mentioned|Fig.6|||||||||
9021|Jones Creek shale|63238|6|Mentioned|p7, p21|||Informal name. ||||||
9021|Jones Creek shale|63240|6|Mentioned|p4|||Referred to as Jones Creek shale sequence.||||||
73322|Jones Creek shale horizon|63238|6|Mentioned|p13|||Informal name. Sedimentary rocks incorporated into the Kershaw Pumice Formation. ||||||
35848|Joyce "Group"|23326|6|Mentioned|974|||Of Spry (1957) - also known as Joyce Metamorphic Complex, but due to similarity with Franklin Metamorphic Complex this name should be discarded due to redundancy.||||||18-APR-07
81723|Joyce Group''|12179|5|Briefly described|p974|||Nomenclature of Spry (1957). Very similar in structural and metamorphic history to Franklin Group; fault-bounded slices of the same lithologies and are in close proximity. See also Joyce Metamorphic Complex; however both terms have been made obsolete.||||||
35837|Joyce Metamorphic Complex|12179|6|Mentioned|p974|||Nomenclature of Turner (1989). Obsolete: see Franklin Metamorphic Complex.||||||
35837|Joyce Metamorphic Complex|23326|5|Briefly described|974|||Originally called Joyce "Group" (Spry 1957 -  but due to similarity with Franklin Metamorphic Complex this name should be discarded due to redundancy.||||||18-APR-07
35837|Joyce Metamorphic Complex|63167|5|Briefly described|p37, p38|||The term Metamorphic Complex was substituted for Group which was invalidly used by previous workers. In the structural order of Metamorphic Complexes (M.C.) Joyce forms the base, overlain by Mary M.C. See also p39.||||||
35837|Joyce Metamorphic Complex|69873|6|Mentioned|p88|||Spry (1957), Turner (1989). Superseded name for the lower part of the currrent Franklin Metamorphic Complex.||||||
35837|Joyce Metamorphic Complex|69874|6|Mentioned|p104|||Turner (1989). Originally the Joyce Group (Spry,1957). Here included with the Franklin Metamorphic Complex of Turner (1989) in a redefinition of that latter unit.||||||
9043|Jubilee Range sequence|41908|6|Mentioned|p45|||||||||
9042|Jubilee Range sequence""|41908|6|Mentioned|p45|||||||||
9051|Judith Formation""|40890|6|Mentioned|p52|||||||||
9051|Judith Formation""|43131|6|Mentioned|Fig.9,p582|||||||||
9051|Judith Formation""|63238|5|Briefly described|p20 Fig. 3|||Informal - see Judith Formation. At base of "Lower Dundas Group".||||||
9051|Judith Formation""|63240|6|Mentioned|p4|||Formerly part of "lower Dundas Group" (lower section) - now redesignated as Western Volcano-Sedimentary Sequence.||||||
9051|Judith Formation""|64395|5|Briefly described|p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Of the Dundas Group (lower part).||||||07-FEB-11
9053|Judith Slate""|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tas. See also p224.||||||24-JUN-08
73801|Judith"" Formation|638|5|Briefly described|p88 Fig. 4.2|Middle Cambrian|Middle Cambrian|Informal - see Judith Formation. ||||||
9056|Jukes Breccia|638|5|Briefly described|p104|||Of Hills (1914a). Occurs at the base of the Owen Conglomerate in some areas. ||||||
9056|Jukes Breccia|22551|6|Mentioned|p149|||||||||
9056|Jukes Breccia|24601|6|Mentioned|p840|||Underlies lower conglomerate member of Owen Conglomerate.||||||30-NOV-09
9056|Jukes Breccia|29875|6|Mentioned|Fig.7|||||||||
9056|Jukes Breccia|29914|6|Mentioned|p12|||||||||
9056|Jukes Breccia|30032|6|Mentioned|Fig.1|||||||||
9056|Jukes Breccia|30277|6|Mentioned|p212|||Refers Hills and Carey(1949)||||||
9056|Jukes Breccia|30889|6|Mentioned|p24|||||||||
9056|Jukes Breccia|31174|6|Mentioned|Fig. 36|||Ordovician||||||
9056|Jukes Breccia|33218|6|Mentioned|Fig.4|||||||||
9056|Jukes Breccia|34502|6|Mentioned|Fig.7|||Lower Ordovician||||||
9056|Jukes Breccia|35153|6|Mentioned|p185|||||||||
9056|Jukes Breccia|36053|6|Mentioned|p435|||See also Fig.1.||||||
9056|Jukes Breccia|36054|6|Mentioned|p437|||||||||
9056|Jukes Breccia|36817|6|Mentioned|p25|||||||||
9056|Jukes Breccia|37044|6|Mentioned|Fig.8|||||||||
9056|Jukes Breccia|37047|6|Mentioned|p247|||||||||
9056|Jukes Breccia|40736|6|Mentioned|p1343|||||||||
9056|Jukes Breccia|63170|6|Mentioned|p189|||||||||07-FEB-11
28628|Jukes Conglomerate""|35844|6|Mentioned|p53|||Informal - see Jukes Conglomerate.||||||24-MAY-07
28628|Jukes Conglomerate""|43054|6|Mentioned|p9|||Refers to Wade and Solomon (1958).||||||25-OCT-07
28628|Jukes Conglomerate""|63169|6|Mentioned|p163|||Of Hills (1913). At base of the Owen sequence (?) - and consists of coarse volcaniclastic breccia and conglomerate. ||||||
28628|Jukes Conglomerate""|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Middle Cambrian|Informal name. Of the Owen Group.||||||25-OCT-07
9058|Jukes Formation|638|5|Briefly described|p104|||See also the informal "Jukes Formation". Names inappropriate due to incorrect correlation with base of Owen Conglomerate (Jukes Breccia); subsequent work shows it is younger than the Tyndall Group. ||||||
9058|Jukes Formation|30276|6|Mentioned|p16|||||||||
9058|Jukes Formation|30278|6|Mentioned|p180|||Late Cambrian age. Probably no longer included in Junee Group?||||||22-MAY-07
9058|Jukes Formation|30281|5|Briefly described|p10|||||||||
9058|Jukes Formation|32794|5|Briefly described|p606|||||||||
9058|Jukes Formation|33218|6|Mentioned|p11|||||||||
9058|Jukes Formation|33839|6|Mentioned|Fig.3|||||||||
9058|Jukes Formation|35118|6|Mentioned|p428|||||||||
9058|Jukes Formation|37046|6|Mentioned|p231|||||||||
9058|Jukes Formation|37047|6|Mentioned|p247|||||||||
9058|Jukes Formation|63169|5|Briefly described|p157 Fig. 5.2|Late Cambrian|Late Cambrian|Geological Province: Dundas Trough.||||||26-OCT-07
9058|Jukes Formation|63170|5|Briefly described|p189|||Succession of volcaniclastic conglomerate and sandstone.||||||07-FEB-11
9058|Jukes Formation|63238|6|Mentioned|p7|||Should be Jukes Conglomerate??||||||
9057|Jukes Formation""|638|5|Briefly described|p104|||See also Jukes Fm. - name inappropriate due to incorrect correlation with base of Owen Conglomerate (Jukes Breccia); subsequent work shows it is younger than the Tyndall Group. Thickness: >250m. Volcaniclastic conglomerate and sandstone with minor tuffs ||||||
9057|Jukes Formation""|22551|6|Mentioned|p149|||||||||
9057|Jukes Formation""|35844|6|Mentioned|p57|||Refers Corbet et al.1974||||||
9057|Jukes Formation""|39892|6|Mentioned|p28|||||||||
9057|Jukes Formation""|40070|6|Mentioned|p12|||||||||
9057|Jukes Formation""|43054|5|Briefly described|p9|||Supersedes/or precedes Jukes Conglomerate?||||||22-MAY-07
9060|Jukes formation|37045|6|Mentioned|p219|||||||||
9060|Jukes formation|40736|6|Mentioned|Fig.1|||||||||
9060|Jukes formation|41148|6|Mentioned|Fig.2|||||||||
9062|Jukes"" Formation|35791|6|Mentioned|Fig.2|||Middle & Late Cambrian correlation chart for Tas.||||||
9080|Junee "Series"|36047|6|Mentioned|p363|||||||||
25724|Junee Group|24548|4|Described|p6|Ordovician|Ordovician|Underlain by Dundas Group (unconformable). Max Thickness: ~2300ft. See also Maps 4687 and 46-88||||||21-MAY-07
25724|Junee Group|29973|5|Briefly described|p107|||||||||
25724|Junee Group|30275|6|Mentioned|p112|||||||||
25724|Junee Group|30277|1|Redefined|p214|Late Ordovician|Late Cambrian|Probably Upper Cambrian to Upper Ordovician||||||
25724|Junee Group|30278|6|Mentioned|p174|||Stratigraphy||||||
25724|Junee Group|30279|6|Mentioned|p121|||See also P122||||||
25724|Junee Group|30280|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|30521|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|30598|6|Mentioned|p50|||||||||
25724|Junee Group|30718|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|30889|6|Mentioned|p23|||||||||
25724|Junee Group|30927|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|31174|6|Mentioned|Fig. 38|||Ordovician||||||
25724|Junee Group|31462|6|Mentioned|p379|||See also Fig.2. Ord.-Camb.||||||
25724|Junee Group|31463|6|Mentioned|Fig.1|||||||||
25724|Junee Group|31464|4|Described|p373|||Stratigraphy||||||
25724|Junee Group|31467|6|Mentioned|p118|||||||||
25724|Junee Group|31472|6|Mentioned|Table 1|||||||||
25724|Junee Group|31477|4|Described|p85|||See also p86-90.||||||21-MAY-07
25724|Junee Group|31648|6|Mentioned|p35|||See also p38. Silurian||||||21-MAY-07
25724|Junee Group|32093|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|32627|6|Mentioned|p21, p22|||See also p37.||||||07-FEB-08
25724|Junee Group|33220|6|Mentioned|p4|||||||||
25724|Junee Group|33348|5|Briefly described|p135|||Ordovician - Lower Silurian.||||||21-MAY-07
25724|Junee Group|33625|6|Mentioned|p187|||||||||
25724|Junee Group|33839|4|Described|p575|||||||||
25724|Junee Group|33840|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|33864|6|Mentioned|p36|||||||||
25724|Junee Group|34287|6|Mentioned|p71|||Ord.||||||
25724|Junee Group|35092|6|Mentioned|p108|||||||||
25724|Junee Group|35118|6|Mentioned|p428|||||||||
25724|Junee Group|35153|6|Mentioned|Fig.1|||||||||
25724|Junee Group|35155|6|Mentioned|Table.1|||Reference Elliston (1954) Blissett (1962).||||||
25724|Junee Group|35203|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|35819|4|Described|p7|||||||||
25724|Junee Group|35828|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|36054|6|Mentioned|p437|||||||||
25724|Junee Group|36122|6|Mentioned|p11|||||||||
25724|Junee Group|37044|6|Mentioned|Fig.1|||||||||
25724|Junee Group|37053|6|Mentioned|p394|||||||||
25724|Junee Group|39235|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25724|Junee Group|40136|5|Briefly described|p28|||||||||
25724|Junee Group|40708|5|Briefly described|p95|||||||||
25724|Junee Group|40760|5|Briefly described|Fig.1|||||||||
25724|Junee Group|41694|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
25724|Junee Group|41934|6|Mentioned|Map legend|Ordovician||||||||
25724|Junee Group|42478|6|Mentioned|p3|||Used Banks (1957), Made redundant 1975.||||||
25724|Junee Group|73369|6|Mentioned|p309, p320|Ordovician|Ordovician|||||||
9081|Junee Group conglomerate|31477|4|Described|p88|||||||||
9082|Junee Group""|29973|6|Mentioned|p107|||||||||
9082|Junee Group""|30277|6|Mentioned|p208|||Stratigraphy||||||
9082|Junee Group""|30279|6|Mentioned|p121|||||||||
9082|Junee Group""|42478|6|Mentioned|p3|||||||||
9084|Junee Series|29973|6|Mentioned|p107|||||||||
9084|Junee Series|36379|6|Mentioned|p201|||||||||
9084|Junee Series|41793|6|Mentioned|p46|||||||||
9083|Junee Series""|29973|6|Mentioned|p108|||||||||
9083|Junee Series""|30275|6|Mentioned|p112|||||||||
9083|Junee Series""|30277|6|Mentioned|p211|||Refers Lewis(1940)||||||
9083|Junee Series""|30279|6|Mentioned|p121|||Refers Lewis(1940)||||||
9083|Junee Series""|41793|6|Mentioned|p46|||||||||
9083|Junee Series""|42478|5|Briefly described|p2|||Used by Lewis (1940)||||||
73248|Junee group|63244|5|Briefly described|p1|Ordovician|Ordovician|Informal name. Includes the Gordon limestone. Underlies Eldon group. Includes the Gordon limestone (topmost bed).||||||08-MAY-07
9086|Junee limestone|29973|6|Mentioned|p107|||||||||
9085|Junee limestone""|30279|6|Mentioned|p125|||Refers Lewis(1940)||||||
79307|Jurassic dolerite|65647|5|Briefly described|Appendix p12|Jurassic|Jurassic|Pipes and dykes of tholeiitic dolerite intrusions, becoming sheet-like at various levels in the Parmeener Supergroup from near the base. Intrudes Bundella Formation, caps the Knocklofty Formation. Caused contact metamorphic effects (hornfelsing and minor wollastonite skarns).||||||
79307|Jurassic dolerite|69876|5|Briefly described|p290, p295, p319-320|Jurassic|Jurassic|Associated metamorphism.||||Intrudes Oonah Formation, Mainwaring Group, Tyndall Group, Mathinna Supergroup.|Dolerite.|
79307|Jurassic dolerite|69878|4|Described|p385-406|Jurassic|Jurassic|Sills and dykes up to about 500m thick, and minor coeval lava, dominate central and eastern Tasmania. Includes Eureka cone sheet, Red Hill granophyre (intrusion), Mt Wellington sheet, Great Lake sheet, Fingal Tier sheet, Quoin intrusion, Glenorchy intrusion. Vertical columnar joints form cliffs and scree. Detached fragment of Ferrar Magmatic Province from Antarctica to SE Australia, associated with Gondwana break-up. Re/Os age 175.1 +/- 5.4 Ma. Chilled margin petrography, mineralogy, geochemistry described in detail. Images. Excellent source of aggregate for road making and concrete.|K/Ar 156-183 Ma. Mean estimate 177.7 +/- 6.2 Ma|||Intrudes Parmeener Supergroup.|Quartz-normative tholeiitic basaltic andesite; pyroxene, plagioclase, mesostasis of quartz, K-feldspar, Fe-Ti oxide; no Mg-olivine; dark fine-grained chilled hornfelsed margin rich in magnetite-ilmenite; granophyric pegmatites.|
79307|Jurassic dolerite|69879|4|Described|p412-413, p430, p439-442, p445-449|Jurassic|Jurassic|See also p453-456, p460-461, p464, p466, p473, p481-484. May intrude Durroon Sub-basin. Also Tasmanian Dolerite, Tasmanian Jurassic dolerites, Jurassic Dolerite. Sequence seismic interpretations. Jurassic dolerite-derived boulder conglomerates are interbedded with Macquarie Harbour Formation. Called 'hybrid rock' when metamorphosed by Cygnet Alkaline Complex.||||Intrudes Parmeener Supergroup. Intruded by Cygnet Alkaline Complex.|Dolerite.|
79307|Jurassic dolerite|69880|5|Briefly described|p516, p518, p545, p548|Jurassic|Jurassic|Mentioned as moraine boulders used to establish ages for glaciation events, by thickness of weathering rinds. Lateritic weathering has produced bauxite deposits: mostly small with no significant production. Source of gravel for construction.||||||
31331|KING ISLAND granite 31331|35828|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
81141|Kamberg Limestone|70194|6|Mentioned|p299 Fig 2|Middle Ordovician|Middle Ordovician|||Unit of Gordon Group||Lowermost unit of the Gordon Group. Overlain by Cashions Creek Limestone. Underlain by Denison Group.||
9244|Kanona adamellite|32301|6|Mentioned|p240|||||||||
9251|Kansas Creek Beds|23837|6|Mentioned|p440 Fig.2|||||||||
9251|Kansas Creek Beds|30150|6|Mentioned|Fig.5|||||||||
9251|Kansas Creek Beds|30155|6|Mentioned|p457|||||||||
9251|Kansas Creek Beds|34099|6|Mentioned|p30|||||||||
9251|Kansas Creek Beds|35268|6|Mentioned|p19|||||||||
9251|Kansas Creek Beds|35288|6|Mentioned|p54|||||||||
9251|Kansas Creek Beds|36788|6|Mentioned|Fig.4|||||||||
9251|Kansas Creek Beds|36817|6|Mentioned|p63|||||||||
9251|Kansas Creek Beds|39777|6|Mentioned|p145|||||||||
9251|Kansas Creek Beds|43474|14|Not recorded|p55,92||Permian|Of the Upper Quamby Group or lower Golden Valley Group.||||||23-MAY-07
9252|Kansas Creek Formation|30819|6|Mentioned|p108|||||||||
9252|Kansas Creek Formation|42000|6|Mentioned|Fig.5 P59|||||||||
73132|Kanunnah Subgroup, lower|44135|6|Mentioned|p8|Mesoproterozoic|Mesoproterozoic|Informal - see Kannunah Subgroup.||||||07-DEC-09
25107|Karmberg Formation|36047|6|Mentioned|Table 3|||||||||
25107|Karmberg Formation|41954|6|Mentioned|Table 1 P12|||||||||
9363|Keel Formation|40070|6|Mentioned|p18|||||||||
9363|Keel Formation|41795|4|Described|p63|||||||||
9363|Keel Formation|41896|6|Mentioned|p27|||Same as Keel Quartzite.||||||23-MAY-07
73359|Keith Beds|63167|5|Briefly described|p22|||Of McNeil (1960). Stated to be included in Keith Metamorphics. See Keith beds also.||||||23-MAY-07
9385|Keith Metamorphics|30197|5|Briefly described|p599|||||||||
9385|Keith Metamorphics|30325|5|Briefly described|p123|||||||||
9385|Keith Metamorphics|30877|4|Described|p25|||See also p26. Proterozoic||||||23-MAY-07
9385|Keith Metamorphics|33348|5|Briefly described|p135|||Precamb.||||||
9385|Keith Metamorphics|33839|5|Briefly described|p567|||||||||
9385|Keith Metamorphics|35288|4|Described|p31|||||||||
9385|Keith Metamorphics|36046|6|Mentioned|p353|||||||||
9385|Keith Metamorphics|38157|6|Mentioned|p286|||||||||
9385|Keith Metamorphics|42358|5|Briefly described|p59|||||||||
9385|Keith Metamorphics|63167|5|Briefly described|p14, p22|Precambrian|Precambrian|Of Gee (1967a,b, 1971, 1977); part of the Arthur Metamorphic Complex. Between Rocky Cape Group and Burnie Formation. Stated to include Keith Beds.||||||23-MAY-07
9385|Keith Metamorphics|69873|6|Mentioned|p78|||Northern part of Arthur Metamorphic Complex.||||Correlative of Timbs Group.||
9386|Keith Schists|39475|6|Mentioned|p404|||||||||
73358|Keith beds|63167|6|Mentioned|p23|||See also Keith Beds.||||||
9387|Keith metamorphics|38638|6|Mentioned|p1901|||||||||
9388|Keith schists|38638|6|Mentioned|p1902|||||||||
9389|Kelcey Tier Beds|23837|6|Mentioned|p440 Fig.2|||||||||
9389|Kelcey Tier Beds|30150|6|Mentioned|Fig.5|||||||||
9389|Kelcey Tier Beds|30155|6|Mentioned|Fig.33.4|||||||||
9389|Kelcey Tier Beds|34323|6|Mentioned|p121|||Permian||||||
9389|Kelcey Tier Beds|36788|6|Mentioned|Fig.4|||||||||
9389|Kelcey Tier Beds|43084|5|Briefly described|p141|Permian|Permian|Thickness: 180m. Interbedded mudstone, pebbly mudstone, siltstone and sandstone.||||||04-DEC-08
9389|Kelcey Tier Beds|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
9389|Kelcey Tier Beds|63868|6|Mentioned|p20|||May be overlapped by Cygnet Coal Measures correlates including Jackey Shale and Clog Tom Sandstone.||||||07-FEB-11
9389|Kelcey Tier Beds|67543|5|Briefly described|p145 Fig.4|||Fig.4 suggests correlation with Abels Bay, Ferntree and Toarra Formations; and with Bogan Gap, Poatina, Middle Arm and Ferntree Groups.|||||Poorly fossiliferous pyritic mudstone.|
25114|Kelcey Tier mudstone|34322|6|Mentioned|p96|||Permian. See also p97.||||||23-MAY-07
9427|Kempton Seam|40334|6|Mentioned|Fig.13|||||||||
23694|Kent Bay granite|36374|3|Fully described|p58|||||||||
73633|Kent Bay/Passage Island Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Compound name for combined granites of Kent Bay Granite and Passage Island Granite. Both of the Boobyalla Suite. S-type, felsic granites; weakly to moderately fractionated, reduced.||||||24-SEP-07
40008|Kentish Spilite|24548|6|Mentioned|p11|||Interfingers with Warner Siltstone. Probably Ordovician?||||||
40009|Kentish Spilite and Volcanic Breccia|24548|5|Briefly described|Map 4687|Cambrian|Cambrian|Of the Dundas Group. Informal name for Kentish Spilite, and Kentish Volcanics.||||||23-MAY-07
78551|Keppel Creek Siltstone|67502|6|Mentioned|p117|||Probable misspelling of Keppel Creek Formation.||||||16-DEC-13
78552|Kepple Creek Siltstone|67502|6|Mentioned|p58|||Kepple Creek Siltstone' (sic) of Matthews (1961b). This term is resurrected, adapted and adopted for the dominantly clastic sedimentary component of the Kanunnah Subgroup, the Keppel Creek Formation.||||||
9473|Kerrison Volcanics""|31475|6|Mentioned|p85|||||||||
73324|Kershaw Pumice Formation""|63238|5|Briefly described|p10|||Informal name - see Kershaw Pumice Formation. A major pumice breccia unit lying at top of Central Volcanic Complex. ||||||
23696|Key Bay granite|36374|3|Fully described|p55|||||||||
9593|King Island Beds|31468|6|Mentioned|p13|||||||||
9593|King Island Beds|37933|6|Mentioned|p549|||||||||
77500|King Island Granitoid|61411|6|Mentioned|p3.|Neoproterozoic|Neoproterozoic|Syn-kinematic intrusion dated 760 +/- 12 Ma.||||||
77500|King Island Granitoid|61412|6|Mentioned|p51.|Neoproterozoic|Neoproterozoic|Syn-kinematic intrusion aged 760 +/- 12 Ma.||||||
77500|King Island Granitoid|73118|6|Mentioned|p72|||Provides the oldest metamorphic event E of the Tasman Line in Tasmania: 760 +/- 12 Ma (Black et al., 1997).||||||
9594|King Island Mixtite|37933|6|Mentioned|p549|||||||||
9596|King Island Volcanics|36198|6|Mentioned|p325|||||||||
9597|King Island biotite lamprophyre|33349|6|Mentioned|p687|||||||||
34033|King Island granite|22603|6|Mentioned|p96|Cryogenian|Cryogenian|Age: 820 Ma.||||||02-JUL-08
34033|King Island granite|22705|5|Briefly described|p792|||Informal name .||||||
34033|King Island granite|64746|6|Mentioned|p388.|||[Formal name is King Island Granite.] Western Tasmanian Terrane. Intrudes Mesoproterozoic metasedimentary rocks.|780-750 Ma.|||||30-MAR-12
68802|King Island granites|24512|6|Mentioned|p7|||Informal name.||||||
9598|King Island lamprophyre|40811|6|Mentioned|p320|||||||||
81327|King Island metamorphics|70025|6|Mentioned|p2|||King Island.||||||
76763|King Island metasandstone|64722|6|Mentioned|Fig. 2 p3-6|Ectasian|Ectasian|Informal name.||||||
9683|Knocklofty Sandstone|32799|6|Mentioned|p27|||||||||
9683|Knocklofty Sandstone|45042|6|Mentioned|p25|||||||||
9682|Knocklofty Sandstone and Shale|24548|3|Fully described|p10|Triassic|Triassic|Formerly the Knocklofty Sandstones (of Johnston and Morton, 1890). Probably an informal name. See also Maps 4687 and 46-88||||||04-JUN-07
9682|Knocklofty Sandstone and Shale|31706|6|Mentioned|p671|||Correlation chart of the Gondwana System.||||||23-MAY-07
9682|Knocklofty Sandstone and Shale|33406|6|Mentioned|p97|||Sample locations.||||||
9682|Knocklofty Sandstone and Shale|35280|6|Mentioned|p143|||||||||
9682|Knocklofty Sandstone and Shale|43876|14|Not recorded|p587||Triassic|Spelt 'Knocklofty sandstone and shale' on reference card by Kummel 1961a.||||||
28647|Knocklofty Sandstone and Siltstone|35280|6|Mentioned|p144|||||||||
28647|Knocklofty Sandstone and Siltstone|63172|5|Briefly described|p316|||Of Camp and Banks (1978). Description suggests this is the lower section of the Knocklofty Formation? Thickness: 185m. Assumed to overlie the Mountain Lodge Member; underlies Poets Road Member.||||||07-FEB-11
28647|Knocklofty Sandstone and Siltstone|63868|6|Mentioned|p24|||Mentioned in terms of equivalents. Probably an informal name but see also Knocklofty Formation - names used interchangeably.||||||07-FEB-11
9684|Knocklofty Sandstones and Shales|23837|6|Mentioned|p442|||Geological Province: Tasmania Basin.||||||
9684|Knocklofty Sandstones and Shales|24549|5|Briefly described|Map 4885|Triassic|Triassic|||||||
9684|Knocklofty Sandstones and Shales|35236|6|Mentioned|p7|||||||||
9684|Knocklofty Sandstones and Shales|39059|6|Mentioned|p590|||||||||
9684|Knocklofty Sandstones and Shales|43895|14|Not recorded|p120|||||||||
9685|Knocklofty Shale|32799|6|Mentioned|p27|||||||||
9685|Knocklofty Shale|40633|6|Mentioned|Fig.1-B|||||||||
83234|Knoklofty Formation|73327|5|Briefly described|Map legend|Triassic|Triassic|||Upper Parmeener Supergroup|||Freshwater, predominantly cross-bedded, quartzose to feldspathic sandstone, commonly with overturned cross-bedding, and subordinate micaceous siltstone.|
39915|Kopanica Shales|24549|6|Mentioned|Map 4885|||Max Thickness: 15ft. Name used interchangeably with Kopanica Formation.||||||23-MAY-07
81285|Kununnah Subgroup|68271|6|Mentioned|p697|||NW Tasmania.|||Includes Croles Hill Diamictite.|||
9999|Lady Barren Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
75273|Lake Timk Dolomite|42227|5|Briefly described|p35|||Probably misspelt - see Lake Timk Formation.||||||
10167|Langloh Seam A|40334|6|Mentioned|Fig.13|||||||||
10168|Langloh Seam B|40334|6|Mentioned|Fig.13|||||||||
10169|Langloh Seam C|40334|6|Mentioned|Fig.13|||||||||
10232|Launceston Beds|31678|6|Mentioned|p98|||||||||
10232|Launceston Beds|31680|6|Mentioned|p174|||||||||
10232|Launceston Beds|32058|6|Mentioned|p124|||Refers Longman et al.(1964)||||||
10232|Launceston Beds|33294|6|Mentioned|p64|||||||||
10232|Launceston Beds|33295|6|Mentioned|p64|||||||||
10232|Launceston Beds|43088|5|Briefly described|p29|||||||||
73356|Lawson River Siltstone|63167|5|Briefly described|p15|Precambrian|Precambrian|Includes siltstone, slate, pyritic slate, impure quartzite and subordinate, but locally common, "greywacke".||||||
73356|Lawson River Siltstone|67502|6|Mentioned|p31, p43, p145|||Name considered redundant: rocks now included in the Cowrie Siltstone. Prospective for good quality slate.||||||
73356|Lawson River Siltstone|69873|6|Mentioned|p43|||Superseded by Cowrie Siltstone.||||||
73133|Layered Dunite-Harzburgite|44135|5|Briefly described|p15|||One of three ultramafic-mafic rock associations with igneous layering within the western part of Dundas region.||||||07-DEC-09
73133|Layered Dunite-Harzburgite|63168|5|Briefly described|p71|||Ultramafic rock association in western Tasmania.||||||
73134|Layered Pyroxenite-Dunite|44135|5|Briefly described|p15|||Informal name. One of three ultramafic-mafic rock associations with igneous layering within the western part of Dundas region.||||||07-DEC-09
73134|Layered Pyroxenite-Dunite|63168|5|Briefly described|p71|||Ultramafic rock association in western Tasmania.||||||
73135|Layered Pyroxenite-Peridotite|44135|5|Briefly described|p15|||Informal name. Shallow marine sequence of thin bedded, pink to grey, bioturbated sandstone and siltstone.||||||07-DEC-09
73135|Layered Pyroxenite-Peridotite|63168|5|Briefly described|p71|||Ultramafic rock association in western Tasmania.||||||
28676|Lemonthyme Basal Tillite|30524|6|Mentioned|Table 2|Pleistocene||Lithostratigraphical relationships.||||||04-JUN-07
10333|Lemonthyme Formation|30524|6|Mentioned|Table 2||Pleistocene|Lithostratigraphical relationships.||||||04-JUN-07
10333|Lemonthyme Formation|40439|6|Mentioned|p375|||||||||
10333|Lemonthyme Formation|69879|5|Briefly described|p449, p505-506|Neogene|Paleogene|Macphail et al. (1993). Occurs below northwestern extent of Central Plateau. Attributed to valley glaciation. Also Lemonthyme tillite. Fossils.|||||Tillite.|
10334|Lemonthyme Rhythmites|30524|6|Mentioned|Table 2|Pleistocene||Lithostratigraphical relationships.||||||04-JUN-07
10346|Leonardsburg Siltstone|30889|6|Mentioned|p23|||Now included in the Cambrian sequence.||||||
78479|Lewis Creek Volcanics|67654|6|Mentioned|p81 Fig.20, p86|Middle Cambrian|Middle Cambrian|See also Lewis River Volcanics in this paper.||||||
73728|Lewis River Volcanics""|63612|5|Briefly described|p7|||Of Whyte (1975) - for an eastern belt of felsic volcanic rocks. Includes basal siliciclastic conglomerate and sandstone.||||||07-FEB-11
73879|Liffey Formation|24552|5|Briefly described|p6|||See also Liffey Sandstone, Liffey Group. Non-marine. Of the Lower Parmeener Supergroup. Geological Province: Tasmania Basin.||||||07-FEB-11
27822|Liffey Sandstone|23837|6|Mentioned|p440 Fig.2|||||||||
27822|Liffey Sandstone|24547|4|Described|p16|Permian|Permian|Overlies the Macrae Mudstone. Maximum Thickness: 35m.||||||
27822|Liffey Sandstone|24548|3|Fully described|p8|Permian|Permian|Conformably overlain by Woodbridge Formation; conformably underlain by Golden Valley Formation. Max Thickness: 250ft. Pale brown and rarely pink massive sandstone with sparkling quartz and some interbedded micaceous shale. See also Map 4687||||||04-JUN-07
27822|Liffey Sandstone|24552|5|Briefly described|p5 Fig.2|Sakmarian|Sakmarian|See also Liffey Formation, Liffey Group. Overlies Massey Creek Group. Geological Province: Tasmanian Basin.||||||07-FEB-11
27822|Liffey Sandstone|30150|6|Mentioned|p99|||||||||
27822|Liffey Sandstone|30155|6|Mentioned|p461|||||||||
27822|Liffey Sandstone|30156|4|Described|p39|||Considered a horizontal marker throughout North Tasmania.||||||30-JAN-08
27822|Liffey Sandstone|30887|6|Mentioned|Map legend|Permian|Permian|||||||
27822|Liffey Sandstone|30889|4|Described|p48|||||||||
27822|Liffey Sandstone|31195|6|Mentioned|Map legend|Permian|Permian|||||||
27822|Liffey Sandstone|31871|6|Mentioned|p9|||Permian||||||
27822|Liffey Sandstone|32290|6|Mentioned|p74|||Top of Liffey Group.||||||04-JUN-07
27822|Liffey Sandstone|33498|6|Mentioned|p48|||Refers Gulline (1973)||||||
27822|Liffey Sandstone|34098|6|Mentioned|p128|||See also pp130,132 etc.||||||04-JUN-07
27822|Liffey Sandstone|34099|6|Mentioned|Fig.1|||Permian.||||||04-JUN-07
27822|Liffey Sandstone|35268|6|Mentioned|p14|||||||||
27822|Liffey Sandstone|36207|6|Mentioned|Text Fig.2|||||||||
27822|Liffey Sandstone|36788|6|Mentioned|p32|||||||||
27822|Liffey Sandstone|38200|6|Mentioned|p75|||||||||
27822|Liffey Sandstone|39579|6|Mentioned|p14|||||||||
27822|Liffey Sandstone|39777|6|Mentioned|p145|||||||||
27822|Liffey Sandstone|41699|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27822|Liffey Sandstone|41895|6|Mentioned|p29|||||||||
27822|Liffey Sandstone|42244|6|Mentioned|p20|||||||||
27822|Liffey Sandstone|43084|5|Briefly described|p140|||Of the Lower Parmeener Supergroup.||||||04-JUN-07
27822|Liffey Sandstone|45042|6|Mentioned|p35|||Permian. Plate 1||||||
27822|Liffey Sandstone|46849|6|Mentioned|p197|||||||||
27822|Liffey Sandstone|63172|5|Briefly described|p302, p337|Permian|Permian|Characterised by well-sorted, quartz-rich, cross-bedded sandstone with washouts, pods of thin siliceous congolmerate and, in places, scattered siliceous pebbles. Used as building sandstone - known as "Patersonia Stone" at Nunamara.||||||07-FEB-11
27822|Liffey Sandstone|63263|6|Mentioned|p55|||May be misnamed - Liffey group is probably correct name?||||||07-FEB-11
27822|Liffey Sandstone|63890|5|Briefly described|p11, p13-14|Permian|Permian|Mentioned in terms of a Permian equivalent . See also p22.||||||
27822|Liffey Sandstone|69773|6|Mentioned|p34|Permian|Permian|Early Bernacchian age from Substage 3b microflora.||||||
74127|Liffey Sandstones and Shales|63820|5|Briefly described|Map legend|Permian|Permian|||||||
10388|Liffey sandstones|32627|6|Mentioned|p25|Permian|Permian|See also p26.||||||07-FEB-08
39315|Liffey-Faulkner Group coals|24408|6|Mentioned|p35|||Informal name.||||||03-MAR-05
73635|Lisle Granite|61216|6|Mentioned|p24|||Referred to only as the Lisle body.||||||10-FEB-11
73635|Lisle Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Diddleum Suite, Scottsdale Batholith.  I-type granite, mafic, unfractionated, oxidised. Name implied from map legend.||||||25-SEP-07
73635|Lisle Granite|73514|5|Briefly described|p1, p5-6, p9-10|Devonian|Devonian|[Written as Lisle granite throughout and Lisle granodiorite on p6, p9-10; probably a variation on Lisle Granodiorite].||||||
10480|Little Chalky Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
10480|Little Chalky Island Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite. I-type, mafic to felsic granite; unfractionated to weakly  fractionated, reduced. Name implied from map legend.||||||25-SEP-07
10480|Little Chalky Island Granite|69876|5|Briefly described|p306 Tb 6.1|Carboniferous|Devonian|Age inferred.||Wybalenna Suite|||I-type granite.|
25170|Little Owen andesite|35844|4|Described|p43|||Petrology||||||
73729|Little Rocky River granite|63612|5|Briefly described|p8|||Informal name. Has an extensive metamorphic aureole to its north. Mentioned informally (p17).||||||07-FEB-11
10534|Lobster Creek "Volcanics"|35791|5|Briefly described|p227|||Refs Burns(1964). 1 of 5 major stratigraphic units in Cambrian Dial Range Trough||||||04-JUN-07
10534|Lobster Creek "Volcanics"|39892|6|Mentioned|Fig.1|||||||||
83423|Lobster Creek Intrusives|69842|6|Mentioned|p6|Cambrian|Cambrian|Riana map; Herrmann (1993) and others.||||Correlated with Riana Dolerite.||
81366|Lobster Creek volcanics|70274|5|Briefly described|p450|Cambrian|Cambrian|Intrusion within the Northern Mount Read Volcanics, with U-Pb SHRIMP zircon age of 500.2+\-7 Ma.|500.2+\-7 Ma|||||
75741|Lohrey's Gully Sandstone and Calcareous Mudstone|66172|14|Not recorded|23|Permian|Permian|||||||
73650|Lone Pine Granite|63540|5|Briefly described|Map legend||Devonian|One of the west  Tasmanian granites. Presented as the compound name - Birthday/Lone Pine (granite). S-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||26-SEP-07
69574|Long Point Granodiorite|61723|5|Briefly described|p811, p810 Tb. 1|Devonian|Devonian|A foliated, enclave-bearing, I-type hornblende-biotite granodiorite/monzogranite that intrudes the Mathinna Supergroup. Age: 395.7+/-2.3Ma. Of the Blue Tier Batholith. ||||||
69574|Long Point Granodiorite|66575|5|Briefly described|p936 Fig.2, p942 Fig5, p951 Tb.2,|Eifelian|Emsian|I-Type; mafic, unfractionated; U-Pb SHRIMP age of 396 +/-2 Ma. Inherited zircons discussed.||||||
10626|Long Point granodiorite|40660|6|Mentioned|Fig.7 p211|||||||||
10633|Longford clay|34994|6|Mentioned|Fig.91|||||||||
10660|Lords Formation|36047|6|Mentioned|Table 3|||||||||
10662|Lords Siltstone|23187|6|Mentioned|p239|||||||||
10662|Lords Siltstone|35819|6|Mentioned|p8|||||||||
10662|Lords Siltstone|36047|5|Briefly described|p365|||||||||
10662|Lords Siltstone|40127|6|Mentioned|p10|||||||||
10662|Lords Siltstone|40136|5|Briefly described|p30|||||||||
10662|Lords Siltstone|40727|6|Mentioned|Fig.3|||||||||
10662|Lords Siltstone|41951|6|Mentioned|p85|||||||||
10662|Lords Siltstone|41954|6|Mentioned|p9|||||||||
10662|Lords Siltstone|42107|6|Mentioned|p306|||||||||
10662|Lords Siltstone|42381|6|Mentioned|p85|||||||||
10662|Lords Siltstone|63170|5|Briefly described|p199, p206|||Thin and apparently discontinuous.Thickness: 15m. Comprises micaceous siltstone and fine sandstone with calcareous nodules, and beds of dark grey to black micritic limestone. Details of fossil fauna  included.||||||07-FEB-11
79579|Lorinna Formation|69879|6|Mentioned|p449|Neogene|Paleogene|Macphail et al. (1993). Occurs below northwestern extent of Central Plateau. Attributed to valley glaciation.||||||
33479|Lottah Alkali-Feldspar Granite|61216|5|Briefly described|p44|Late Devonian|Late Devonian|Of McClenaghan and Williams (1982). Name used interchangeably with Lottah Granite - probably informal.One of two main alkali-feldspar bodies in Blue Tier Batholith, the other being Mt Paris Granite.Dominantly K-feldspar.||||||10-FEB-11
33479|Lottah Alkali-Feldspar Granite|63171|5|Briefly described|p260|||Alkali-feldspar body with sheet-like form and includes equigranular and quartz and K-feldspar porphyritic varieties having gradational relationships with each other. In the Blue Tier batholith.||||||24-SEP-07
77660|Lottah Pluton|67804|5|Briefly described|p69|Late Devonian|Late Devonian|[The word Pluton is being used as a synonym for the Granite]|377 +/- 3 Ma (U-Pb zircon: Black 2004).|||Intrudes Mathinna Supergroup.|Highly-fractured S-type granite.|
25178|Lottah alkali feldspar granite|39927|6|Mentioned|p311|||||||||
28693|Low Rocky Point granite|41143|6|Mentioned|p277|||||||||
29806|Lower Dundas Group""|43054|5|Briefly described|p26|||||||||
10737|Lower Freshwater Sequence|42320|6|Mentioned|p12|||Unintentional formalisation of "Lower Freshwater Sequence"?||||||
10737|Lower Freshwater Sequence|63263|4|Described|p34, p61|||Informal strat.name used extensively in discussion of Lower Parmeener Group.Comprises Faulkner Gp in S.or Liffey Gp, Mersey + Preolenna C.M. in N.Tasmania. Overlies Woody I. Siltst./Quamby Mudst.- Bundella Fm - Golden Valley Gp sequence.Thick:20-40m.||||||07-FEB-11
10737|Lower Freshwater Sequence|69877|5|Briefly described|p363|Permian|Carboniferous|Of Clarke and Banks (1975), who divided the (now Parmeener Supergroup) succession according to depositional environment. This unit is equivalent to part of the Lower Parmeener Supergroup.|||||Mostly non-marine sandstone and coal.|
10736|Lower Freshwater Sequence""|30819|6|Mentioned|p107|||||||||
10738|Lower Freshwater beds|40694|6|Mentioned|p7|||||||||
10765|Lower Limestone Member|23187|5|Briefly described|Fig2p237|Eastonian|Darriwilian|||||||
10765|Lower Limestone Member|42416|6|Mentioned|p194|||?Informal Member of Benjamin Limestone.||||||
10765|Lower Limestone Member|42478|6|Mentioned|p7|||||||||
10765|Lower Limestone Member|43668|6|Mentioned|Fig.8,p12|||||||||
10765|Lower Limestone Member|50091|5|Briefly described|p413 Tb. 1, p414 Tb. 2|Late Ordovician|Late Ordovician|Name abbreviated to Low L/st Mem in Table 1.  Occurrence of Panderodus nogamii (conodonts) - in the Florentine Valley .||||||04-NOV-04
10765|Lower Limestone Member|69875|4|Described|p243 Fig 5.2, p246, p251-255|Late Ordovician|Middle Ordovician|Images and descriptions of fossils. Geochemistry briefly described. Correlations with unnamed limestone occurrences listed.||Benjamin Limestone||Underlies Lords Siltstone Member. Overlies Cashions Creek Limestone.|Peritidal carbonates, dominantly micrite limestone, 600m, 5-20m thick cyclical prograding tidal flats.|
10768|Lower Marine Sequence|42320|6|Mentioned|p12|||Unintentional formalisation of "Lower Marine Sequence"?||||||
10768|Lower Marine Sequence|69877|5|Briefly described|p363|Permian|Carboniferous|Of Clarke and Banks (1975), who divided the (now Parmeener Supergroup) succession according to depositional environment. This unit is equivalent to part of the Lower Parmeener Supergroup.|||||Glaciomarine and fossiliferous marine deposits.|
10767|Lower Marine Sequence""|30819|6|Mentioned|p107|||||||||
26706|Lower Parmeener Super-Group|32059|6|Mentioned|Map legend|Permian|Permian|||||||
26706|Lower Parmeener Super-Group|35818|4|Described|p7|||||||||
26706|Lower Parmeener Super-Group|35819|4|Described|p10|||||||||
26706|Lower Parmeener Super-Group|37405|5|Briefly described|p29|||||||||
26706|Lower Parmeener Super-Group|37477|6|Mentioned|p492|||||||||
26706|Lower Parmeener Super-Group|39680|6|Mentioned|Map legend|Permian|Permian|||||||
26706|Lower Parmeener Super-Group|40694|4|Described|p7|||||||||
26706|Lower Parmeener Super-Group|43072|5|Briefly described|p14|||||||||
26706|Lower Parmeener Super-Group|43088|6|Mentioned|p26|||||||||
26706|Lower Parmeener Super-Group|69854|5|Briefly described|Map legend|Permian|Permian|Fossil associations listed.|||Includes Boullanger, Skipping Ridge, Counsel Creek, Marra and Toarra Formations and Darlington Limestone.|||
10795|Lower Parmeener Supergroup|73320|5|Briefly described|Map legend|Permian|Carboniferous|Overlies angular unconformity.||||Underlies Upper Parmeener Supergroup.|Glacial, glaciomarine and non-marine sedimentary rocks; includes pebbly mudstone, pebbly sandstone and limestone; freshwater and paralic sandstone and mudstone with some coal; minor tasmanite oil shale in lower part; basal tillite.|
10795|Lower Parmeener Supergroup|73321|5|Briefly described|Map legend|Permian|Permian||||Woody Island Siltstone, Bundella Formation, Faulkner Group, Harts Hill Limestone, Nassau Siltstone, Deep Bay Formation, Malbina Formation, Risdon Sandstone, Abels Bay Formation.|Underlies the Upper Parmeener Supergroup|Includes glaciomarine mudstone, siltstone and sandstone, calcareous siltstone and limestone, variably fossiliferous to unfossiliferous, in places contains pebbly layers, lonestones, bioturbation; in part contact metamorphosed by dolerite.|
10795|Lower Parmeener Supergroup|73322|5|Briefly described|Map legend|Permian|Permian||||Woody Island Siltstone, Bundella Formation, Faulkner Group, Cascades Group,|Underlies the Upper Parmeener Supergroup.||
10795|Lower Parmeener Supergroup|73323|5|Briefly described|Map legend|Permian|Permian||||Woody Island Siltstone, Bundella Formation, Faulkner Group, Berriedale Limestone, Nassau Siltstone, Rayner Sandstone, Deep Bay Formation, Malbina Formation, Risdon Sandstone, Abels Bay Formation|Underlies the Upper Parmeener Supergroup.|Includes variably bedded siltstones and sandstones, marine to glaciomarine and variably fossiliferous, contains lodestones and is pebble-rich in places; lesser fossiliferous limestones; in part contact metamorphosed by Jurassic dolerite.|
10795|Lower Parmeener Supergroup|73324|6|Mentioned|Map legend|||||||||
10795|Lower Parmeener Supergroup|73326|5|Briefly described|Map legend|Permian|Permian||||Malbina Formation, Risdon Sandstone, Abels Bay Formation.|Underlies the Upper Parmeener Supergroup.|Includes poorly fossiliferous, glaciomarine sandstone and interbedded non-fissile to fissile siltstone and silty sandstone, common bioturbation, lonestones and pebble rich patches, also includes richly fossiliferous beds and cobble-rich layers.|
10795|Lower Parmeener Supergroup|73327|5|Briefly described|Map legend|Permian|Permian||||Bundella Formation, Faulkner Group, Hickman Formation, Berridale Limestone, Nassau Siltstone, Rayner Sandstone, Deep Bay Formation, Malbina Formation, Risdon Sandstone, Abels Bay Formation.|Underlies the Upper Parmeener Supergroup|Includes fossiliferous to unfossiliferous, predominantly glaciomarine siltstone, mudstone and sandstone, some containing lonestones and pebble-rich patches; lesser calcareous siltstone and limestone; contact metamorphosed by dolerite.|
10795|Lower Parmeener Supergroup|73328|5|Briefly described|Map legend|Permian|Permian||||Malbina Formation, Risdon Sandstone, Abels Bay Formation.|Underlies the Upper Parmeener Supergroup.|Includes generally poorly fossiliferous, glaciomarine interbedded sandstone and fissile to non-fissile siltstone and silty sandstone, contains lonestones, bioturbation, pebble rich patches and fossiliferous beds in parts.|
10853|Lughrata Sand|33358|4|Described|Table 1|||||||||
10856|Luina Beds|23718|6|Mentioned|p39|||||||||
10856|Luina Beds|37056|6|Mentioned|Fig.1|||||||||
10856|Luina Beds|69874|6|Mentioned|p111|||Rubenach (1973), Ford (1981). Subsequently the Luina Group (Corbett et al., 2014). ||||||
10855|Luina Beds""|41795|6|Mentioned|p34|||||||||
10855|Luina Beds""|63168|6|Mentioned|p57|||Of Rubenach (1973). Informal name. In Cleveland-Waratah area.||||||
10879|Lyell Schists|41695|6|Mentioned|Map legend|Cambrian||||||||
10879|Lyell Schists|43164|6|Mentioned|23||Middle Devonian|||||||
10879|Lyell Schists|63238|6|Mentioned|p9|||||||||
10879|Lyell Schists|73170|6|Mentioned|p787|Late Cambrian|Middle Cambrian|Local name for the Central Volcanic Complex.||||||
10878|Lyell Schists""|30278|5|Briefly described|p176|||||||||
10878|Lyell Schists""|32794|6|Mentioned|p608|||||||||
10880|Lyell schists""|35844|3|Fully described|p28|||Refers to Wade and Solomon 1958.||||||
10880|Lyell schists""|63169|6|Mentioned|p165|Devonian|Devonian|Informal name for volcanic sequences at Mt Lyell.||||||
10880|Lyell schists""|69874|5|Briefly described|p201|||A large (7 x 1 km) N-S oriented zone, focussed along the Great Lyell Fault. Hosts the Mount Lyell Cu mineralisation. Complex relationships with the Owen Group.|||||Hydrothermally altered volcanics.|
10881|Lymingtonian Stage|30150|2|Defined|p99|Late Permian|Early Permian|Early-Late Permian||||||
10881|Lymingtonian Stage|38906|4|Described|p13|||||||||
10881|Lymingtonian Stage|38908|6|Mentioned|p6|||||||||
10881|Lymingtonian Stage|39680|6|Mentioned|Map legend|Permian|Permian|||||||
26710|Lynch Creek "Basalts"|30278|6|Mentioned|p179|||Cross section||||||
26710|Lynch Creek "Basalts"|41695|6|Mentioned|Map legend|Cambrian||||||||
10882|Lynch Creek Basalts""|30278|6|Mentioned|p183|||Refers to Solomon(1960). Correlation||||||
10882|Lynch Creek Basalts""|32794|6|Mentioned|p608|||||||||
10884|Lynch Creek andesites|37045|6|Mentioned|p219|||||||||
73325|Lynch Creek basalt|63238|6|Mentioned|p8|||Informal name. Presented as Lynch Creek basalt body. ||||||
10885|Lynch Creek basalt""|40070|6|Mentioned|p11|||||||||
10887|Lynch Creek basalts|638|6|Mentioned|p114|||Informal name. ||||||
10887|Lynch Creek basalts|35844|3|Fully described|p24, Fig. 12|Cambrian|Cambrian|Of the Mount Read Volcanics. See also "Lynch basalts". See also p29.||||||24-MAY-07
10887|Lynch Creek basalts|37045|6|Mentioned|p214|||||||||
10887|Lynch Creek basalts|43131|5|Briefly described|p570,p574|||informal name.||||||15-MAY-07
10887|Lynch Creek basalts|63169|6|Mentioned|p161|||Informal name for basalts near Queenstown - occur along the western flank of the Mount Read belt. . ||||||
10887|Lynch Creek basalts|64395|5|Briefly described|p172|||Informal name. Together with Howards Plains intrusives, Hellyer Creek basalts and possibly Sock Creek basalts, these rocks form Suite 3 of Mount Read Volcanics.||||||07-FEB-11
10886|Lynch Creek basalts""|35844|3|Fully described|p14|||See also see Lynch basalts.||||||24-MAY-07
73802|Lynchford tuffs|638|6|Mentioned|p113 Fig. 4.11, p114|||Informal name for a component within the Mount Read Volcanics.||||||30-JAN-08
10929|MacRae Mudstone|34099|6|Mentioned|Fig.1|||Permian.||||||06-FEB-08
10943|Mackenzie Conglomerate|37412|6|Mentioned|p24|||||||||
10950|Mackintosh crystal tuff|36817|6|Mentioned|p128|||||||||
76017|Macquarie Harbour beds|66858|6|Mentioned|p980.|||Named by Scott (1960); given status of Formation in this article.||||||
40187|Macquarie Island ophiolite|23995|6|Mentioned|p351|||In the SW Pacific region.||||||
40187|Macquarie Island ophiolite|49914|4|Described|p12-13|||Informal name.  A unique ophiolite occurrence on Macquarie Island  in the Southern Ocean ~1500km south-southeast of Tasmania.  Age: 12-9.5m.y.||||||
10965|Macrae Formation|24547|5|Briefly described|p21|||See Macrae Mudstone. Conformably overlain by Liffey Sandstone. Conformably overlies Billop Sandstone.||||||11-MAY-04
10965|Macrae Formation|30156|5|Briefly described|p38|||Part of Golden Valley Group.||||||06-FEB-08
10965|Macrae Formation|63172|5|Briefly described|p308 Fig. 10|||Informally use name on chart (Fig. 8.10). - see Macrae Mudstone.||||||07-FEB-11
10965|Macrae Formation|63263|5|Briefly described|p33 Fig. 7|||Misnamed and should be Macrae Mudstone.||||||07-FEB-11
73355|Magg's Quartzite|63167|5|Briefly described|p37|Precambrian|Precambrian|Of Spry (1958b). Incorporated into Fisher Group by Jennings (1963) but unclear whether or not the name remains in current usage? ||||||
11009|Magnet Creek Lithic Sandstone Formation|30293|6|Mentioned|p629|||||||||
73336|Magog Basalt|63249|5|Briefly described|p2|||Geological Province: Fossey Mountain Trough (Dundas Trough).||||||
11013|Magog Group|30277|6|Mentioned|p212|||||||||
11013|Magog Group|31195|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11013|Magog Group|32627|6|Mentioned|p11 Fig. 3|Ordovician|Ordovician|||||||07-FEB-08
11013|Magog Group|34012|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11013|Magog Group|36788|6|Mentioned|p25|||||||||
78482|Mainwaring Basalts""|67654|6|Mentioned|p9|||Now Montgomery Basalt.||||||
73426|Mainwaring Group""|63168|5|Briefly described|p57, p58|||Of Hall and Corbett (1968). Name never properly defined but used in numerous company reports. Succession of volcano-sedimentary rocks - lithology included. Max. thickness: 3000m. ||||||
73426|Mainwaring Group""|67654|6|Mentioned|p9, p47, p80|||Now a sub-group of the Luina Group. Now Montgomery Basalt. Considered to be a correlate of the Miners Ridge Basalt (now Guilfoyle Basalt).||||||
73426|Mainwaring Group""|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Elliott Bay-Queenstown-Rosebery region.||||Correlative of Luina Group.|Mafic volcaniclastic sandstone-siltstone-mudstone-chert-minor carbonate sequences, with intercalated tholeiitic basalt flows; considered allochthonous.|
73426|Mainwaring Group""|73320|6|Mentioned|Map legend|Cambrian Series 2|Terreneuvian|Dundas, Fossey Mountains and Dial Range Troughs. Included in map unit of Luina Group and correlates with description of mafic volcaniclastic sandstone-siltstone-mudstone-chert-minor carbonate sequences, with intercalated tholeiitic basalt flows. Considered allochthonous. Uncertainty indicated for Terreneuvian age.||||Correlate of Luina Group.||
73137|Mainwaring River Volcanics|44135|6|Mentioned|p23|||Part of the collective name, Birchs Inlet-Mainwaring River Volcanics (Brown et al 1991) for a basaltic volcanic association in two areas: one in Birchs Inlet and the other in a belt trending north from near Veridian Point on west coast.||||||07-DEC-09
37829|Mainwaring River volcanics|24216|6|Mentioned|p815|||||||||
79497|Mainwaring Volcanics|69874|6|Mentioned|p113-114, p116|||See also references to Mainwaring Group (p110, p116-117). Geochemistry briefly described.||||||
11070|Malbina A|49644|5|Briefly described|Table|||?beds ?Member ?||||||29-MAY-08
11071|Malbina Beds|33711|6|Mentioned|Table 1|||||||||
11073|Malbina E|49644|5|Briefly described|Table|||?Member ?beds ?Formation||||||
11072|Malbina E beds|39267|6|Mentioned|p241|||||||||
11074|Malbina Formation (upper)|41474|6|Mentioned|p59|||||||||
11076|Malbina Member A|30155|6|Mentioned|p464|||||||||
11077|Malbina Member E|30155|6|Mentioned|p464|||||||||
11077|Malbina Member E|40694|6|Mentioned|p11|||||||||
11077|Malbina Member E|63172|6|Mentioned|p306|||Informal reference to the upper section of Malbina Formation - characterised by molluscan-dominated faunas including the giant clam Megadesmus grandis in abundance in the first instance then followed by biocoemotic assemblages of spinose strophomenids.||||||07-FEB-11
11078|Malbina Sandstone|30153|6|Mentioned|Fig.45|||||||||
11078|Malbina Sandstone|30327|6|Mentioned|p165|||||||||
11078|Malbina Sandstone|34099|6|Mentioned|Fig.1|||Perm.||||||
11078|Malbina Sandstone|34287|6|Mentioned|p129|||Permian||||||
11078|Malbina Sandstone|43084|6|Mentioned|p91|||||||||
25197|Malbina Sandstone and Siltstone|33711|6|Mentioned|Table 1|||||||||
11080|Malbina Siltstone|30153|6|Mentioned|Fig.45|||||||||
11080|Malbina Siltstone|34099|6|Mentioned|Fig.1|||Perm.||||||
11080|Malbina Siltstone|34494|6|Mentioned|p52|||||||||
11080|Malbina Siltstone|43084|6|Mentioned|p91|||Of Lower Parmeener Supergroup.||||||29-MAY-08
11079|Malbina Siltstone and Sandstone|31461|4|Described|p51|||||||||
11079|Malbina Siltstone and Sandstone|34047|6|Mentioned|p83|||Permian.||||||29-MAY-08
11079|Malbina Siltstone and Sandstone|66174|14|Not recorded|?|||||||||
11081|Malbina formation|33302|6|Mentioned|Fig.1,2|||||||||
39192|Marrawah Limestone|23768|6|Mentioned|p71|Longfordian|Longfordian|||||||
26726|Mary Ann Bay sandstone|31762|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
11403|Mary Group|30616|4|Described|p191|||See Map on p192.||||||19-SEP-07
11403|Mary Group|45087|5|Briefly described|p224|||Chem. analyses. See also p235.||||||19-SEP-07
83232|Maryann Bay Sandstone|73321|6|Mentioned|Map legend|||Possibly equivalent to an unnamed Quaternary unit described as poorly consolidated conglomerate derived from Permian mudstone, and fine-grained sandstone.||||||
11448|Mathinna Beds|20374|14|Not recorded|118-119|||||||||
11448|Mathinna Beds|23231|6|Mentioned|Fig5-4p51|||||||||
11448|Mathinna Beds|23522|5|Briefly described|p246|Middle Devonian|Early Devonian|||||||
11448|Mathinna Beds|23850|6|Mentioned|p786|||See Mathinna Group.||||||
11448|Mathinna Beds|23923|5|Briefly described|p1216 Fig 1.|Early Devonian|Ordovician|||||||
11448|Mathinna Beds|29607|5|Briefly described|p32|||||||||
11448|Mathinna Beds|30280|6|Mentioned|Map legend|Tremadocian|Cambrian|Lower Devonian - Tremadocian - Cambrian||||||
11448|Mathinna Beds|30521|6|Mentioned|Map legend|Tremadocian|Cambrian|Lower Devonian Tremadocian - Cambrian||||||
11448|Mathinna Beds|30718|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11448|Mathinna Beds|30813|5|Briefly described|p87|||Silurian - Devonian. Cu sulphides in fault zones.||||||
11448|Mathinna Beds|30879|6|Mentioned|p48|||Contact with pluton. Map P49.||||||
11448|Mathinna Beds|30885|6|Mentioned|p42|||Silurian-Devonian age||||||
11448|Mathinna Beds|30887|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
11448|Mathinna Beds|30889|3|Fully described|p39|||See also P40-45||||||
11448|Mathinna Beds|30927|6|Mentioned|Map legend|Silurian|Cambrian|Lower Devonian to Cambrian||||||
11448|Mathinna Beds|31138|6|Mentioned|p632|||||||||
11448|Mathinna Beds|31173|4|Described|p10|||See also Fig. 1. Sil.-Dev.||||||
11448|Mathinna Beds|31176|5|Briefly described|p11|||||||||
11448|Mathinna Beds|31178|6|Mentioned|p29|||Tin & Gold in quartz veins.||||||
11448|Mathinna Beds|31179|6|Mentioned|p363|||||||||
11448|Mathinna Beds|31185|6|Mentioned|Fig. 1|||Siluro - Devonian||||||
11448|Mathinna Beds|31435|6|Mentioned|p40|||||||||
11448|Mathinna Beds|31464|6|Mentioned|p373|||||||||
11448|Mathinna Beds|31520|6|Mentioned|p27|||||||||
11448|Mathinna Beds|31525|6|Mentioned|Fig. 1|||||||||
11448|Mathinna Beds|31765|5|Briefly described|p32|||||||||
11448|Mathinna Beds|31766|6|Mentioned|p64|||||||||
11448|Mathinna Beds|31772|6|Mentioned|p64|||||||||
11448|Mathinna Beds|31773|6|Mentioned|p65|||Refers rock vibration||||||
11448|Mathinna Beds|31790|5|Briefly described|p4|||Early Ord. - Early Dev.||||||
11448|Mathinna Beds|31791|6|Mentioned|p14|||See also P15, 16||||||
11448|Mathinna Beds|31829|6|Mentioned|p29|||Palaeozoic||||||
11448|Mathinna Beds|31832|6|Mentioned|p52|||||||||
11448|Mathinna Beds|31871|6|Mentioned|p6|||Silurian||||||
11448|Mathinna Beds|32064|6|Mentioned|p253|||||||||
11448|Mathinna Beds|32093|6|Mentioned|Map legend|Tremadocian|Cambrian|L.Dev.-Tremadocian-Cambrian (?)||||||
11448|Mathinna Beds|33218|6|Mentioned|p11|||||||||
11448|Mathinna Beds|33220|6|Mentioned|Fig.2|||||||||
11448|Mathinna Beds|33326|6|Mentioned|p439|||Fauna.||||||
11448|Mathinna Beds|33348|4|Described|p135|||Ord.-L.Dev.||||||
11448|Mathinna Beds|33358|6|Mentioned|p153|||Sil.-Dev.||||||
11448|Mathinna Beds|33497|6|Mentioned|p31|||||||||
11448|Mathinna Beds|33732|4|Described|p108|||||||||
11448|Mathinna Beds|33839|4|Described|p576|||||||||
11448|Mathinna Beds|33840|6|Mentioned|Map legend|Tremadocian|Cambrian|Lower Devonian - Tremadocian - Cambrian||||||
11448|Mathinna Beds|34098|6|Mentioned|p135|||||||||
11448|Mathinna Beds|34263|6|Mentioned|p14|||||||||
11448|Mathinna Beds|34264|6|Mentioned|p48|||Ord.- Dev.||||||
11448|Mathinna Beds|34287|6|Mentioned|p84|||See also P99||||||
11448|Mathinna Beds|34315|6|Mentioned|p27|||Ord.- Dev. See also P29||||||
11448|Mathinna Beds|34316|4|Described|p16|Devonian|Early Ordovician|See also pp17-20. Detailed lithology presented. Intruded by Scottsadale Granite - see p55.||||||06-FEB-08
11448|Mathinna Beds|34365|6|Mentioned|p125|||See also P126||||||
11448|Mathinna Beds|34385|6|Mentioned|p38|||Ordovician - Devonian||||||
11448|Mathinna Beds|34596|6|Mentioned|p362|||See also PP388,389. Silurian - Devonian.||||||
11448|Mathinna Beds|34994|6|Mentioned|p249|||||||||
11448|Mathinna Beds|35153|6|Mentioned|Fig.1|||||||||
11448|Mathinna Beds|35203|6|Mentioned|Map legend|Cambrian|Cambrian|Silurian - Devonian Early?||||||
11448|Mathinna Beds|35300|6|Mentioned|Fig.1|||||||||
11448|Mathinna Beds|35303|6|Mentioned|p253|||||||||
11448|Mathinna Beds|35818|5|Briefly described|p6|||||||||
11448|Mathinna Beds|35821|6|Mentioned|Map legend|Devonian|Silurian|||||||
11448|Mathinna Beds|35824|6|Mentioned|Map legend|Silurian|Silurian|Prob. Silurian||||||
11448|Mathinna Beds|35825|4|Described|p163|||||||||
11448|Mathinna Beds|35826|6|Mentioned|p121|||||||||
11448|Mathinna Beds|35827|4|Described|p13|||||||||
11448|Mathinna Beds|35828|6|Mentioned|Map legend|Silurian|Cambrian|Devonian-Silurian-Ordovician-Cambrian||||||
11448|Mathinna Beds|35864|6|Mentioned|p307|||||||||
11448|Mathinna Beds|35912|6|Mentioned|Fig.1|||||||||
11448|Mathinna Beds|36374|4|Described|p50|||||||||
11448|Mathinna Beds|36534|6|Mentioned|p226|||||||||
11448|Mathinna Beds|36787|6|Mentioned|Map legend|Devonian|Silurian|Devonian-Silurian-Ordovician||||||
11448|Mathinna Beds|37044|6|Mentioned|Fig.4|||||||||
11448|Mathinna Beds|37797|4|Described|p148|||||||||
11448|Mathinna Beds|37801|6|Mentioned|p113|||||||||
11448|Mathinna Beds|39579|3|Fully described|p8|||See also P16||||||
11448|Mathinna Beds|39677|6|Mentioned|Map legend|Devonian|Silurian|Devonian to Silurian||||||
11448|Mathinna Beds|39777|6|Mentioned|p137|||||||||
11448|Mathinna Beds|39892|5|Briefly described|p30|||||||||
11448|Mathinna Beds|39916|6|Mentioned|Map legend|Devonian|Silurian|Devonian - Silurian||||||
11448|Mathinna Beds|39927|6|Mentioned|p306|||||||||
11448|Mathinna Beds|40073|6|Mentioned|p131|||||||||
11448|Mathinna Beds|40127|6|Mentioned|p11|||||||||
11448|Mathinna Beds|40136|6|Mentioned|p16|||||||||
11448|Mathinna Beds|40310|6|Mentioned|p249|||See also Fig.5||||||
11448|Mathinna Beds|40334|6|Mentioned|p43|||||||||
11448|Mathinna Beds|40660|6|Mentioned|p201|||||||||
11448|Mathinna Beds|40704|5|Briefly described|p83|||||||||
11448|Mathinna Beds|40760|4|Described|p178|||||||||
11448|Mathinna Beds|41471|5|Briefly described|p288|||||||||
11448|Mathinna Beds|41562|6|Mentioned|Fig.1|||||||||
11448|Mathinna Beds|41639|6|Mentioned|p11|||||||||
11448|Mathinna Beds|41691|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
11448|Mathinna Beds|41692|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
11448|Mathinna Beds|41696|6|Mentioned|Map legend|Devonian|Ordovician|||||||
11448|Mathinna Beds|41795|6|Mentioned|Fig.42|||||||||
11448|Mathinna Beds|41818|4|Described|p6|||||||||
11448|Mathinna Beds|41855|4|Described|p10|||||||||
11448|Mathinna Beds|41909|6|Mentioned|p112|||||||||
11448|Mathinna Beds|42154|6|Mentioned|p338|||||||||
11448|Mathinna Beds|42244|6|Mentioned|p15|||In NE Tasmania.||||||12-AUG-08
11448|Mathinna Beds|42320|6|Mentioned|p8|||||||||
11448|Mathinna Beds|42331|5|Briefly described|p843|||||||||
11448|Mathinna Beds|42348|6|Mentioned|p1|||||||||
11448|Mathinna Beds|42553|6|Mentioned|Map legend|Early Devonian|Ordovician|||||||
11448|Mathinna Beds|42838|5|Briefly described|Fig.1 P375|||||||||
11448|Mathinna Beds|42877|5|Briefly described|p155|||||||||
11448|Mathinna Beds|42878|6|Mentioned|p170|||superseded by Mathinna Group||||||
11448|Mathinna Beds|43078|4|Described|p13|||||||||
11448|Mathinna Beds|43084|5|Briefly described|p68|||||||||
11448|Mathinna Beds|43131|5|Briefly described|p565|||||||||
11448|Mathinna Beds|43191|6|Mentioned|Fig.1 p40.|||||||||
11448|Mathinna Beds|43327|14|Not recorded|p50,51|||||||||
11448|Mathinna Beds|43328|14|Not recorded|p43,47|||||||||
11448|Mathinna Beds|43329|14|Not recorded|p497,498|||||||||
11448|Mathinna Beds|43456|14|Not recorded|p32||Silurian|||||||
11448|Mathinna Beds|43457|14|Not recorded|Map Legend|Devonian|Silurian|||||||
11448|Mathinna Beds|43461|14|Not recorded|p628|||||||||
11448|Mathinna Beds|43488|6|Mentioned|17|||||||||
11448|Mathinna Beds|43547|14|Not recorded|Tb 152,156-8,160-1|Gedinnian||(Skalian-Gedinnian)||||||
11448|Mathinna Beds|43587|6|Mentioned|Fig.1,p162|Devonian|Ordovician|||||||
11448|Mathinna Beds|43594|6|Mentioned|p52|||is this 'informal'||||||
11448|Mathinna Beds|43892|6|Mentioned|p118||Early Devonian|||||||
11448|Mathinna Beds|45922|14|Not recorded|p.518-520|||||||||
11448|Mathinna Beds|48764|6|Mentioned|p113|||||||||
11448|Mathinna Beds|61395|5|Briefly described|p2 Fig. 1.1|Early Devonian|Late Cambrian|Marine quartzwacke trubidite.  In eastern Tasmania.||||||07-FEB-11
11448|Mathinna Beds|63592|6|Mentioned|p41|||Host rock for gold mineralisation.||||||
11448|Mathinna Beds|63635|6|Mentioned|p9|||Of Banks (1962). Superseded by Mathinna Supergroup. ||||||
11448|Mathinna Beds|64393|5|Briefly described|p79, p80|Paleozoic|Paleozoic|Unconformably overlain by Parmeener Supergroup rocks. Quartz/wacke slate turbidite sequence. Contain Early Ordovician graptolites.||||||07-FEB-11
11448|Mathinna Beds|65214|6|Mentioned|p273|Devonian|Devonian|TAS, NE. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
11448|Mathinna Beds|66174|14|Not recorded|?|||||||||
11448|Mathinna Beds|67493|4|Described|p5, p7, p58 Fig.25|Early Devonian|Early Ordovician|Banks (1962), Williams (1978), Baillie et al. (1989); later the Mathinna Group (Powell and Baillie, 1992); subsequently Mathinna Supergroup (Reed, 2001).|||||Arenite-lutite association consisting of sandstone or coarse siltstone grading up into fine siltstone or claystone in most places, the latter being equal or subordinate in thickness to the former.|
11448|Mathinna Beds|67503|6|Mentioned|p18 Fig.5|||Replaced by Mathinna Supergroup - appears on map modified after McClenaghan et al. (1992).||||||
11448|Mathinna Beds|69773|6|Mentioned|p11|Devonian|Ordovician|NE Tasmania.||||||
11448|Mathinna Beds|69852|5|Briefly described|Map legend|Devonian|Ordovician|Age shown as Ordovician(?)-Silurian-Devonian.||||Is overlain unconformably by Parmeener Super-Group.|Contact metamorphic psammite, spotted pelite and minor schist; quartzwacke turbidite sequence.|
11448|Mathinna Beds|69853|5|Briefly described|Map legend|Early Devonian|Ordovician|Age range given as Ordovician(?)-Silurian-Early Devonian(?). Various facies mapped separately. Angular clasts occur within volcanic breccia intersected by a drill hole; and rounded clasts occur in Tertiary silts, sand and gravel and Pleistocene colluvium.||||Is unconformably overlain by the Lower Parmeener Supergroup.|Dominantly mudstone and siltstone; metapsammite, metaquartzite and metapelite contact metamorphosed by granite intrusions; quartzwacke turbidite sequence of interbedded sandstone, siltstone and mudstone, some quartzite units.|
11448|Mathinna Beds|69854|5|Briefly described|Map legend|Devonian|Silurian|Age is shown as ?Siluro-Devonian.||||Is unconformably overlain by Lower Parmeener Super-Group.|Quartzwacke turbidite sequence. Contact metamorphic psammite and spotted pelite.|
11448|Mathinna Beds|69876|6|Mentioned|p277|||Structural trend map of regional cleavage: Goscombe et al. (1994).||||||
11448|Mathinna Beds|69877|6|Mentioned|p381|Devonian|Devonian|Source of some of the pebbles and clasts in the uppermost succession of the Upper Parmeener Supergroup.||||||
11448|Mathinna Beds|73369|5|Briefly described|p298|Late Devonian|Silurian|Age suggested by poorly preserved plant and marine fossils. At least 6000 ft thick.|||||Sequence of sandstone siltstone and mudstone.|14-MAY-22
11445|Mathinna Beds and granites|35825|6|Mentioned|p166|||||||||
11446|Mathinna Beds hornfels|35818|6|Mentioned|p6|||||||||
11446|Mathinna Beds hornfels|35826|5|Briefly described|p124|||||||||
11447|Mathinna Beds""|31790|6|Mentioned|p8|||||||||
11447|Mathinna Beds""|31791|6|Mentioned|p6|||Camb. - Dev.||||||
11449|Mathinna Formation|38200|6|Mentioned|p68|||||||||
11449|Mathinna Formation|65646|6|Mentioned|p66.|||Probably mis-used for Mathinna Supergroup. Turbidites. Hosts most of the goldfields east of the Tamar River. Turbiditic sandstone-slate.||||||09-JAN-15
11450|Mathinna Group|22599|5|Briefly described|p75|||Smithton Basin. 550 m thick.||||||17-JAN-07
11450|Mathinna Group|22603|5|Briefly described|p100|Early Devonian|Early Ordovician|||||||
11450|Mathinna Group|22627|5|Briefly described|p132|Devonian|Ordovician|||||||
11450|Mathinna Group|22668|5|Briefly described|p27||Paleozoic|||||||07-NOV-08
11450|Mathinna Group|23467|4|Described|p281|Early Ordovician|Early Ordovician|||||||
11450|Mathinna Group|23792|5|Briefly described|p22|Early Devonian|Ordovician|Folded quartzwacke turbidites. Geological Province: Lachlan Fold Belt. Intruded by Devonian granites.||||||
11450|Mathinna Group|23850|5|Briefly described|p786|||Previously named Mathinna Beds.||||||26-APR-06
11450|Mathinna Group|24002|6|Mentioned|p226|||||||||
11450|Mathinna Group|24098|5|Briefly described|p27 Fig. 2|Emsian|Early Ordovician|Geological Province: Lachlan Fold Belt (Northeast Tasmania).||||||
11450|Mathinna Group|24220|6|Mentioned|p879|||Superseded by Mathinna Supergroup.||||||
11450|Mathinna Group|24588|5|Briefly described|p10, 17, p31 Fig.15|Emsian|Emsian|Geolgical Province: Lachlan Fold Belt.||||||29-NOV-13
11450|Mathinna Group|30813|6|Mentioned|Fig.1|||Silurian-Devonian age||||||
11450|Mathinna Group|32051|6|Mentioned|p91|||Silurian||||||
11450|Mathinna Group|37044|6|Mentioned|p196|||||||||
11450|Mathinna Group|37405|6|Mentioned|Fig.1|||||||||
11450|Mathinna Group|42878|2|Defined|p195|Early Devonian|Early Ordovician|see also Fig.1, p170.||||||17-JAN-07
11450|Mathinna Group|43326|14|Not recorded|p17,19|||||||||
11450|Mathinna Group|43330|14|Not recorded|p28|||||||||
11450|Mathinna Group|43331|14|Not recorded|p63,64|||||||||
11450|Mathinna Group|43333|14|Not recorded|p106-7,111-2 fig51|||||||||
11450|Mathinna Group|43334|14|Not recorded|p95|||||||||
11450|Mathinna Group|43364|14|Not recorded|p212|||||||||
11450|Mathinna Group|43584|4|Described|p56|Devonian|Ordovician|Graptolite fossils.||||||17-JAN-07
11450|Mathinna Group|43663|6|Mentioned|p6|Early Devonian|Ordovician|||||||
11450|Mathinna Group|44135|5|Briefly described|p29, p41|Devonian|Devonian|Comprises Stony Head Sandstone, Turquoise Bluff Slate, Bellingham Formation and Sidling Sandstone.||||||07-DEC-09
11450|Mathinna Group|45431|6|Mentioned|p1242||Early Paleozoic|||||||07-NOV-08
11450|Mathinna Group|45644|5|Briefly described|Page 1237||Early Paleozoic|||||||07-NOV-08
11450|Mathinna Group|60904|6|Mentioned|p783|||In Tasmania.||||||
11450|Mathinna Group|61260|6|Mentioned|p424|||In eastern Tasmania.||||||
11450|Mathinna Group|61395|4|Described|p5-6|Devonian|Ordovician|Late Cambrian? Max. thick: ~7km. Intruded by granitoid rocks of Scottsdale, Blue Tier + Eddystone Batholiths. See also p4 Fig. 1.3.|||Includes: Stony Head Sst, Turquoise Bluff Slate, Bellingham Fm + Sidling Sst. and Corn Hill Beds||Siliciclastic sedimentary rocks.|17-DEC-13
11450|Mathinna Group|63604|6|Mentioned|p969|||||||||
11450|Mathinna Group|64396|5|Briefly described|p209 Fig. 1, p211|||Includes Stony Head Sandstone, Turquoise Bluff Slate and Bellingham Formation. ||||||
11450|Mathinna Group|65646|6|Mentioned|p4 Fig.1, p56 Fig.30.||Late Cambrian|Includes Stony Head Sandstone, Turquoise Bluff Slate (relationship shown in Fig.1 from Reed 2001 [outdated?]). Probably mis-used instead of Mathinna Supergroup.||||||05-FEB-16
11450|Mathinna Group|66172|6|Mentioned|p25, 23|||Correlated with Scamander Slate and Quartzite||||||09-SEP-10
11450|Mathinna Group|66174|14|Not recorded|?|||||||||
11450|Mathinna Group|67493|4|Described|p5, p6 Fig.1, p7, p8 Fig.2, p9|Early Devonian|Early Ordovician|Of Powell and Baillie (1992), Powell et al. (1993). Superseded: elevated to the status of Supergroup (Reed, 2001). Included Stony Head Sandstone, Turquoise Bluff Slate and Bellingham Formation. Formerly Mathinna Beds (Banks, 1962).|||According to Powell and Baillie (1992): Stony Head Sandstone, Turquoise Bluff Slate and Bellingham Formation are the three lowermost outcropping formations (the base of the sequence is not exposed).|||
11450|Mathinna Group|69581|6|Mentioned|p180|||The West Tasmania Terrane was not contributing sediments (including zircons) to the major Ordovician basins, such as this Group.||||||
11450|Mathinna Group|69872|6|Mentioned|p28,30 Figs.2.11-2.12|||||||||
11450|Mathinna Group|69875|5|Briefly described|p264|||Powell and Baillie (1992). Originally the Mathinna beds of Banks (1962), Williams (1978)[both of which actually used Mathinna Beds], Baillie et al. (1989), for the folded Early Ordovician to Early Devonian sedimentary successions in NE Tasmania. Subsequently the Mathinna Supergroup (Reed, 2001).|||Stony Head Sandstone, Turquoise Bluff Slate, Bellingham Formation, "Sidling sandstone".|Is overlain unconformably by St Marys Porphyrite.||18-SEP-17
11450|Mathinna Group|69876|6|Mentioned|p273, p276, p278|||Powell et al. (1973). Raised to Supergroup status by Reed (2001) on recognition that major deformation event separated lower and upper units of Mathinna Group, Tippogoree and Panama Groups, by inferred unconformity.||||||
11450|Mathinna Group|70025|6|Mentioned|p16|||Eastern Tasmanian Terrane.||||||
11450|Mathinna Group|70194|6|Mentioned|p299 Fig 2, p301, 323|Early Devonian|Early Ordovician|Also referred to as Mathinna Supergroup in text (p299). Basinal turbidite deposition on the Eastern Tasmanian Terrane (dense oceanic crust; Rawlinson et al., 2006).||||Correlative to the Eldon and Gordon groups.|Sandstone and siltstone. |
74081|Mathinna Group, Lower|61395|6|Mentioned|p82|||Informal - see Mathinna Group.||||||07-FEB-11
74082|Mathinna Group, lower|61395|6|Mentioned|p21|||Informal - see Mathinna Group.||||||07-FEB-11
74083|Mathinna Group, upper|61395|6|Mentioned|p18|||Informal - see Mathinna Group.||||||07-FEB-11
32587|Mathinna Series|45643|14|Not recorded|Pages Unknown?|||||||||
74389|Mathinna Slate and Quartzite|63170|5|Briefly described|p234|||Part of the former 'arenite-lutite association' of Banks (1962e) together with Fingal beds and Scamander Quartzite and Slate.||||||07-FEB-11
11451|Mathinna beds|23245|6|Mentioned|p136|||||||||
11451|Mathinna beds|23521|6|Mentioned|p5-3 Fig. 1|||||||||
11451|Mathinna beds|23850|6|Mentioned|p793|||Superseded.||||||
11451|Mathinna beds|24220|6|Mentioned|p879|||||||||
11451|Mathinna beds|29585|6|Mentioned|p17|||||||||
11451|Mathinna beds|30879|6|Mentioned|p48|||Silurian-Devonian. Map P48.||||||
11451|Mathinna beds|31791|4|Described|p3|||||||||
11451|Mathinna beds|31832|6|Mentioned|p52|||||||||
11451|Mathinna beds|34316|6|Mentioned|p34|||||||||
11451|Mathinna beds|35826|6|Mentioned|Fig.22|||||||||
11451|Mathinna beds|39927|6|Mentioned|p303|||||||||
11451|Mathinna beds|42119|6|Mentioned|p524|||||||||
11451|Mathinna beds|42962|6|Mentioned|p73|||||||||
11451|Mathinna beds|43022|5|Briefly described|Fig.3,p474|||||||||
11451|Mathinna beds|43084|5|Briefly described|Fig.14|||||||||
11451|Mathinna beds|43164|6|Mentioned|2|Devonian|Ordovician|||||||
11451|Mathinna beds|43335|14|Not recorded|p91|||||||||
11451|Mathinna beds|61216|5|Briefly described|p48 Fig. 19|||Informal reference to sections of the Mathinna Supergroup rocks.||||||10-FEB-11
11451|Mathinna beds|63168|5|Briefly described|p70 Fig. 3.6|Devonian|Ordovician|||||||
11451|Mathinna beds|63169|5|Briefly described|p154-155|Devonian|Ordovician|Folded turbidite-mudstone sequence. ||||||
11451|Mathinna beds|63170|5|Briefly described|p234-235|Early Devonian|Silurian|Approximates the "Lutite Association" of Banks (1962e). In the Beaconsfield area.||||||07-FEB-11
11451|Mathinna beds|63171|5|Briefly described|p287 Fig. 7.21, p291|Early Devonian|Ordovician|||||||07-MAY-08
11451|Mathinna beds|63172|6|Mentioned|p331|||||||||07-FEB-11
11451|Mathinna beds|63173|6|Mentioned|p369, p370|||Metamorphosed sedimentary rocks.||||||07-FEB-11
11451|Mathinna beds|64396|5|Briefly described|p224 Fig. 18|Early Devonian|Ordovician|May be misspelt - probably intended to be Mathinna Group?||||||08-DEC-08
11451|Mathinna beds|64571|6|Mentioned|p823|Early Paleozoic|Early Paleozoic|||||||
11451|Mathinna beds|69875|5|Briefly described|p244, p264|||Banks (1962), Williams (1978) [both of which actually used Mathinna Beds], Baillie et al. (1989), for the folded Early Ordovician to Early Devonian sedimentary successions in NE Tasmania. Later the Mathinna Group (Powell and Baillie, 1992), then Mathinna Supergroup (Reed, 2001). Eastern Tasmanian Terrane.||||Is overlain unconformably by St Marys Porphyrite.||18-SEP-17
28731|Mathinna sandstone|38200|6|Mentioned|p68|||||||||
11452|Mathinna slate|34994|6|Mentioned|p250|||||||||
11452|Mathinna slate|43335|14|Not recorded|p91|||See also Lexicon||||||
11548|McIvor Hill Gabbro|33853|6|Mentioned|Fig.1|||Cambrian.||||||
11548|McIvor Hill Gabbro|63168|5|Briefly described|p69|Cambrian||||||||
11548|McIvor Hill Gabbro|70274|5|Briefly described|p445,452,462|Series 2|Series 2|Component of the mafic-ultramafic complex interpreted to underlie the Mount Read Volcanics. Zircon analysis gave a weighted average 206Pb/238U age of 516.0+\-0.9 Ma, which is considered to be the crystallization age of the sample, and pre-dates Mount Read Volcanics by about 10my.|516.0+\-0.9 Ma|||||
11551|McIvors Hill Gabbro|37501|6|Mentioned|p407|||||||||
32521|McKellar's Creekton Formation|32627|6|Mentioned|p26|||Of McKellar (1957). Informal or misnamed reference to Creekton Formation.||||||07-FEB-08
11556|McKenzie Conglomerate|29875|6|Mentioned|Fig.7|||||||||
74390|McLeod Formation|63170|5|Briefly described|p225 Fig. 6.12|Lochkovian|Lochkovian|Of Tiger Range Group. Overlies Currawong Quartzite. Thickness: 480m. In the Western Tasmania Terrane. Consists of interbedded mudstone and lesser sandstone; poorly fossiliferous.||||||07-FEB-11
74390|McLeod Formation|69875|4|Described|p258 Fig 5.13, p263|Pragian|Lochkovian|Age inferred from Fig 5.13. Discrepancy in thickness of Formation : 400m or 480m thick.||Tiger Range Group||Overlies Currawong Quartzite conformably.|Interbedded mudstone and lesser sandstone. Poorly fossiliferous with poorly-preserved or fragmentary dalmanitid trilobites, a possible chonetid brachiopod and indeterminate plant remains.|
11579|McRae Formation|24549|4|Described|p8|Permian|Permian|Of the Golden Valley Group. Max Thickness: 120ft. Predominantly mudstone, containing bands of marl up to one foot in thickness||||||22-FEB-07
11579|McRae Formation|34316|5|Briefly described|p21 Fig.3||Early Permian|Of the Golden Valley  Group. Dominantly mudstone.||||||06-FEB-08
11579|McRae Formation|43479|14|Not recorded|p161||Visean|||||||
11594|Meander Formation|24549|4|Described|p7|Permian|Permian|Basal unit of the Woodbridge Group. Overlies the Creekton Formation. Max Thickness: 200ft.||||||06-FEB-08
11594|Meander Formation|32290|6|Mentioned|Fig. 21|||Permian. Of the Poatina Group?||||||19-SEP-07
11594|Meander Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Of the Woodbridge Group. Dominantly mudstone.||||||06-FEB-08
11594|Meander Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
11594|Meander Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
11595|Meander Mudstone Formation|32290|6|Mentioned|Fig. 21|||Not intended as a formal name.  Permian. Of the Poatina Group.||||||19-SEP-07
69577|Medeas Cove Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Poimena Suite, Blue Tier Batholith. I-type granite, felsic, moderately fractionated, reduced. Name implied from map legend.||||||
69577|Medeas Cove Granite|71100|6|Mentioned|p126|||||||||
69577|Medeas Cove Granite|71141|6|Mentioned|p126|||||||||
69577|Medeas Cove Granite|71730|6|Mentioned|p33, p37, p42, p56, p60|||[Formal name intended].|||||I-type granite.|
11659|Meredith Adamellite|35153|6|Mentioned|p199|||||||||
37068|Meredith Group|23718|5|Briefly described|p47|Early Carboniferous|Late Devonian|Age: 353+/-7 Ma.||||||
11661|Meredith adamellite|37053|6|Mentioned|Table 2|||||||||
11662|Meredith granite|33218|6|Mentioned|p31|||||||||
11662|Meredith granite|39361|6|Mentioned|p1441|||||||||
11662|Meredith granite|39717|6|Mentioned|p644|||||||||
11662|Meredith granite|39772|6|Mentioned|p18|||||||||
11662|Meredith granite|61412|6|Mentioned|p32.|||||||||
11663|Meredith microgranite|37053|6|Mentioned|Table 2|||||||||
11664|Meredith porphyritic adamellite|37053|6|Mentioned|Table 2|||||||||
11677|Meridith Granite|39475|6|Mentioned|Fig.1|||Misspelling of Meredith?||||||
40215|Merrideth Granite|24200|5|Briefly described|p425|Paleozoic|Paleozoic|||||||07-NOV-08
11731|Mersey Bluff dolerite|36382|5|Briefly described|p41|||||||||
25231|Mersey Coal beds|32977|6|Mentioned|p559|||||||||
11733|Mersey Group|30340|6|Mentioned|p2525|||||||||
11733|Mersey Group|30341|5|Briefly described|p128|||Permian age||||||
11733|Mersey Group|31461|4|Described|p51|||Permian||||||
11733|Mersey Group|32945|6|Mentioned|p85|||See also p86. Permian.||||||20-SEP-07
11733|Mersey Group|33494|6|Mentioned|p45|||||||||
11733|Mersey Group|33711|6|Mentioned|p382|||||||||
11733|Mersey Group|34099|6|Mentioned|p10|||Broad. Equiv. Faulkner Group.||||||20-SEP-07
11733|Mersey Group|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
11733|Mersey Group|34287|6|Mentioned|p129|||Permian||||||
11733|Mersey Group|35268|6|Mentioned|p9|||||||||
11733|Mersey Group|36788|6|Mentioned|Fig.4|||||||||
11733|Mersey Group|37065|6|Mentioned|p29|||See also p46. [Originally entered for Qld. CEBMar95]||||||20-SEP-07
11733|Mersey Group|63868|6|Mentioned|p21|Early Permian|Early Permian|Non-marine sandstones.||||||07-FEB-11
11733|Mersey Group|66174|14|Not recorded|?|||||||||
78071|Mersey Metamorphic Complex|68253|6|Mentioned|p1008 Fig.1, p1016 Fig.10|Neoproterozoic|Neoproterozoic|||||||
78071|Mersey Metamorphic Complex|69874|5|Briefly described|p97 Fig 4.2, p101 Fig 4.5, p102|||See also p108 Table 4.1. Meffre et al. (2000), for low-grade metamorphic rocks along northern margin of Tyennan Region in upper section of Mersey River and parts of Cradle Mountain area. This study incorrectly attributes the name "Mersey Valley Metamorphic Complex" to Meffre et al. (2000). Shown as Mersey MC in Fig 4.2 and Table 4.1.|Ages range 500 +/- 6 Ma to 456 Ma.|||||
35846|Mersey River Complex|23326|5|Briefly described|977, p979|||Abbreviated version of Mersey River Metamorphic Complex.||||||18-APR-07
11734|Mersey River Granite|22705|6|Mentioned|Fig.2 p791|||||||||
11734|Mersey River Granite|37501|6|Mentioned|p407|||||||||
78072|Mersey River Metamorphics|68253|5|Briefly described|p1015, p1016 Tb.3|Paibian|Guzhangian|North Central region. U-Th-Pb monazite age data from Chmielowski (2009).|ca. 497 +/- 3 Ma|||||20-JUL-15
11735|Mersy Coal Measures|35280|6|Mentioned|p143|||||||||
73327|Merton Road volcaniclastic sequences|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Informal name for rocks within the Huskisson Group - name is invalid.  ||||||
73326|Miners Ridge Basalt|43250|5|Briefly described|Map Legend||Cambrian|Of Yolande River Sequence. Ophitic textured tholeiitic basalt lava, breccia.||||||24-MAY-07
73326|Miners Ridge Basalt|63238|6|Mentioned|p8, p17|||Exposed in the core of the Miners Ridge Anticline near Lynchford. Also presented as Miners Ridge Basalt body. Part of the Yolande River Sequence. ||||||
73326|Miners Ridge Basalt|63612|6|Mentioned|p6|||Near Queenstown.||||||07-FEB-11
73326|Miners Ridge Basalt|64395|5|Briefly described|p168, p172|Middle Cambrian|Middle Cambrian|Appears to be interbedded with Miners Ridge Sandstone. Included in Suite 5 of Mount Read Volcanics. Recent mapping shows Miners Ridge Basalt and Miners Ridge Sandstone to be fault-enclosed suggesting tectonic emplacement. See also p174 Fig. 8||||||07-FEB-11
73326|Miners Ridge Basalt|67654|6|Mentioned|p9, p47, p80|||Replaced by the Guilfoyle Basalt. Considered to be a correlate of the Mainwaring Group"". See Miners Ridge Basalt"".||||||
78483|Miners Ridge Basalt""|67654|5|Briefly described|p47, p80 |||See also Miners Ridge Basalt.||||Underlain by the Mount Read Volcanics.||
78483|Miners Ridge Basalt""|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Adamsfield-Jubilee region.|||||Tholeiitic basalt and picrite.|
11897|Miners Ridge basalt|35844|6|Mentioned|Fig.4|||Informal name.||||||24-MAY-07
11897|Miners Ridge basalt|43131|5|Briefly described|p570,p574|||Informal name (invalid).||||||15-MAY-07
11897|Miners Ridge basalt|43133|6|Mentioned|p601|||informal name. Part of Yolande River sequence.||||||
11897|Miners Ridge basalt|69874|6|Mentioned|p116|||Informal and invalid name: an overlying unit called Miners Ridge Sandstone had precedence. Subsequently the Guilfoyle Creek Basalt.||||||
73803|Miners Ridge basalts|638|5|Briefly described|p85, p106|||Informal name for tholeiitic basalts within the Mount Read Volcanics; also referred to as Miners Ridge tholeiites. See also p114.||||||
73803|Miners Ridge basalts|63169|6|Mentioned|p160|||Informal name for tholeiitic basalts in the Queenstown region. ||||||
11898|Miners Ridge sandstone|35844|3|Fully described|p14|||Informal - see Miners Ridge Sandstone.||||||24-MAY-07
73280|Minnow Keratophyre""|63240|6|Mentioned|p6|||Quartz-feldspar porphyry intrusive.||||||
25242|Minnow Keratophyro|29626|6|Mentioned|Map 160|||||||||
81367|Minnow keratophyre|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Western Volcano-Sedimentary Sequence, with U-Pb SHRIMP zircon age of 499.6+\-11.2 Ma.|499.6+\-11.2 Ma|||||
41359|Minyari Suite|50608|6|Mentioned|p1.1|||||||||
11969|Misery Hill Conglomerate|31572|6|Mentioned|Fig.|||Correlation chart 1. Upper Cambrian||||||20-SEP-07
11969|Misery Hill Conglomerate|42204|6|Mentioned|p233|||||||||
23802|Modder River granite|36374|3|Fully described|p55|||||||||
12018|Moina Formation|41954|6|Mentioned|p3|||||||||
12018|Moina Formation|42557|5|Briefly described|p384|||||||||
12018|Moina Formation|69875|4|Described|p241, p244, p248-250, p255||Ordovician|Apparently used interchangeably with Moina Sandstone. Local difficulties in applying this unit to the Gordon Group are discussed. Proximal shallow-marine and intertidal deposits fringing an emergent basement high. Fossils briefly described: late Darriwilian.||Gordon Group||Overlies Duncan Conglomerate.|Sandy siliciclastics.|18-SEP-17
12019|Moina Pipestem Sandstone|40136|6|Mentioned|p31|||||||||
12020|Moina Quartzite|37054|5|Briefly described|Fig.2|||||||||
12021|Moina Sandstone Formation|41954|6|Mentioned|Fig.5 P8|||||||||
28761|Moina Sandstone""|35791|6|Mentioned|p226|||||||||
28761|Moina Sandstone""|39892|6|Mentioned|p14|||||||||
28761|Moina Sandstone""|42204|6|Mentioned|p233|||||||||
28761|Moina Sandstone""|44135|6|Mentioned|p28|||Informal - see Moina Sandstone.||||||07-DEC-09
73278|Moina conglomerate|63240|6|Mentioned|p5|||Refers to the basal conglomerate of Moina Sandstone where the typical lithology of the sandstone, with trace fossils, is interbedded with pebbly bands nearly to the base of the sequence.||||||10-DEC-07
12022|Moina sandstone|31765|6|Mentioned|p32|||||||||
12022|Moina sandstone|36339|6|Mentioned|p31|||||||||
12022|Moina sandstone|36345|6|Mentioned|p16|||||||||
12022|Moina sandstone|37054|6|Mentioned|p439|||||||||
38771|Molbina Formation|23837|6|Mentioned|p440 Fig.2|||||||||
40345|Montana Basalts|23932|5|Briefly described|p665 Table 1|Early Cambrian|Early Cambrian|Age: ~530 Ma.||||||
12124|Montana Melaphyre|24604|6|Mentioned|p904|||||||||
12124|Montana Melaphyre|33839|6|Mentioned|p569|||||||||
12124|Montana Melaphyre|43191|6|Mentioned|p43|||Another name for Oonah Formation??||||||
12123|Montana Melaphyre Volcanics|31141|6|Mentioned|p4|||||||||
12123|Montana Melaphyre Volcanics|63167|5|Briefly described|p18|||Of Hills and Carey (1949) - term used for high titanium, alkali basalts around the Montana Mine.||||||
12123|Montana Melaphyre Volcanics|63168|6|Mentioned|p50 Tb. 3.1|||Name now obsolete - incorporated into the Oonah Formation.||||||
12122|Montana Melaphyre Volcanics""|41795|6|Mentioned|p12|||||||||
40347|Montana Melaphyre""|23932|6|Mentioned|p675|Neoproterozoic|Neoproterozoic|Of the Oonah Formation.||||||
40347|Montana Melaphyre""|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Adamsfield-Jubilee region. Stated to be within Oonah Formation [as a Member?] near Zeehan.|||||Alkali basalt.|
82820|Montana volcanics|71711|6|Mentioned|p395, p397|||Near Zeehan. Mafic rocks within or equivalent to  the upper part of the Oonah Formation.|||||Basaltic lava flows, pillow basalts and mafic volcaniclastic rocks.|14-DEC-21
78481|Montgomery Basalt""|67654|5|Briefly described|p9, p47|||See also Montgomery Basalt.||||||
12274|Moorabool Viaduct Formation|22944|5|Briefly described|Fig3||Miocene|||||||
12274|Moorabool Viaduct Formation|23230|5|Briefly described|p42|||||||||
12274|Moorabool Viaduct Formation|23239|4|Described|Table1p109, 111-2|Pliocene|Miocene|||||||
12274|Moorabool Viaduct Formation|23242|6|Mentioned|Fig11-4.1p158||Pliocene|||||||
12274|Moorabool Viaduct Formation|23243|5|Briefly described|Fig11-5.1p170, 172, 175||Pliocene|||||||
12274|Moorabool Viaduct Formation|23909|5|Briefly described|p291|Pliocene|Miocene|Of Brighton Group.  Geological Province: Otway Basin.||||||
12274|Moorabool Viaduct Formation|24038|5|Briefly described|p445|Pliocene|Miocene|Geological Province: Torquay Basin||||||
12274|Moorabool Viaduct Formation|24104|5|Briefly described|p149, 152|Pliocene|Late Miocene|Geological Province: Otway Basin.||||||
12274|Moorabool Viaduct Formation|24344|5|Briefly described|p73|||Correlative of Hanson Plain Sand (Bock and Glenie, 1965).||||||
12274|Moorabool Viaduct Formation|24551|6|Mentioned|p305|||||||||
12274|Moorabool Viaduct Formation|29823|6|Mentioned|p14|||||||||
12274|Moorabool Viaduct Formation|29825|5|Briefly described|p18|||||||||
12274|Moorabool Viaduct Formation|30576|6|Mentioned|Table 1|||||||||
12274|Moorabool Viaduct Formation|30578|5|Briefly described|p13|||||||||
12274|Moorabool Viaduct Formation|30579|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
12274|Moorabool Viaduct Formation|30580|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
12274|Moorabool Viaduct Formation|30929|6|Mentioned|Map legend|Pliocene|Miocene|Miocene and Pliocene age||||||
12274|Moorabool Viaduct Formation|31036|6|Mentioned|Table 9-1|||Pliocene||||||
12274|Moorabool Viaduct Formation|34986|6|Mentioned|p330|||||||||
12274|Moorabool Viaduct Formation|35066|4|Described|p215|||||||||
12274|Moorabool Viaduct Formation|40724|6|Mentioned|p97|||||||||
12274|Moorabool Viaduct Formation|41185|6|Mentioned|Fig.4|||||||||
12274|Moorabool Viaduct Formation|41704|6|Mentioned|Fig.3|||||||||
12274|Moorabool Viaduct Formation|41769|4|Described|p36|||||||||
12274|Moorabool Viaduct Formation|41849|6|Mentioned|p404|||||||||
12274|Moorabool Viaduct Formation|42184|6|Mentioned|Fig.2 P348|||||||||
12274|Moorabool Viaduct Formation|42318|6|Mentioned|Fig.1 P10|||||||||
12274|Moorabool Viaduct Formation|42524|5|Briefly described|Fig.3 P27|||||||||
12274|Moorabool Viaduct Formation|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
12274|Moorabool Viaduct Formation|43660|6|Mentioned|Fig.6,p15|Pleistocene|Miocene|||||||
12274|Moorabool Viaduct Formation|48911|6|Mentioned|Chart 1|||||||||
12274|Moorabool Viaduct Formation|50352|5|Briefly described|Map Legend|Tertiary|Tertiary|Very course-grained to pebbly quartz sandstone and ferruginous polymictic conglomerate||||||04-JUN-04
12274|Moorabool Viaduct Formation|61155|5|Briefly described|p18|Pleistocene|Late Pliocene|Geological Province: Otway Basin (Tyrendarra and Port Cambell Empayments) and Aire Embayment. ||||||
12274|Moorabool Viaduct Formation|61207|5|Briefly described|p280 Fig. 2|Early Pliocene|Late Miocene|Basal marine calcareous sands (burrows and marine molluscs) underlie non-calcareous sands and silts of probably non-marine origin. Overlies Fyansford Clay; underlies Newer Volcanics. Age: 5.3-4.9Ma. Geol. Prov: onshore Otway Basin and Port Phillip Basin.||||||
12274|Moorabool Viaduct Formation|61624|6|Mentioned|p465|||Equivalent of Whalers Bluff Formation.||||||07-APR-09
12274|Moorabool Viaduct Formation|61896|5|Briefly described|p57|||Locally unconformably underlies both Port Campbell Limestone and Gellibrand Marl Formation.||||||19-DEC-07
12274|Moorabool Viaduct Formation|64314|5|Briefly described|p502 Fig. 7|||||||||
12274|Moorabool Viaduct Formation|66002|6|Mentioned|p12|||Of Bock and Glenie, 1965. Superseded name. See also Moorabool Viaduct Sand. Replaced by Hanson Plain Sand then Black Rock Sandstone.||||||
12274|Moorabool Viaduct Formation|67061|6|Mentioned|p554 Fig.10.|Pliocene|Pliocene|||||||
25261|Moorabool Viaduct Sand|22875|6|Mentioned|p72|||||||||
25261|Moorabool Viaduct Sand|22886|5|Briefly described|p17|Tertiary|Tertiary|Of Brighton Group.||||||07-MAR-07
25261|Moorabool Viaduct Sand|23768|5|Briefly described|p30 Fig.6, p136|Early Pliocene|Late Miocene|Geological Province: Port Phillip Basin.||||||30-MAR-05
25261|Moorabool Viaduct Sand|24104|5|Briefly described|p151|Pliocene|Miocene|||||||
25261|Moorabool Viaduct Sand|24551|5|Briefly described|p319|||Maximum Thickness: 21m.||||||
25261|Moorabool Viaduct Sand|30818|6|Mentioned|Fig.1|||Lower Pliocene||||||
25261|Moorabool Viaduct Sand|32815|6|Mentioned|p200|||||||||
25261|Moorabool Viaduct Sand|35066|4|Described|p223|||||||||
25261|Moorabool Viaduct Sand|35262|6|Mentioned|p1|||||||||
25261|Moorabool Viaduct Sand|35276|3|Fully described|p241|||||||||
25261|Moorabool Viaduct Sand|35290|4|Described|p44|||See also p40.||||||07-MAR-07
25261|Moorabool Viaduct Sand|35712|6|Mentioned|Table 6|||||||||
25261|Moorabool Viaduct Sand|36499|6|Mentioned|p50|||||||||
25261|Moorabool Viaduct Sand|37385|4|Described|p13|||||||||
25261|Moorabool Viaduct Sand|38144|6|Mentioned|Map legend|Pliocene|Miocene|Miocene to Pliocene||||||
25261|Moorabool Viaduct Sand|38159|6|Mentioned|Map legend|Pliocene|Miocene|Miocene to Pliocene||||||
25261|Moorabool Viaduct Sand|41511|5|Briefly described|p17|||||||||
25261|Moorabool Viaduct Sand|41537|5|Briefly described|p352|||||||||
25261|Moorabool Viaduct Sand|42453|6|Mentioned|p7|||||||||
25261|Moorabool Viaduct Sand|42827|3|Fully described|p315|||Of Brighton Group.||||||07-MAR-07
25261|Moorabool Viaduct Sand|43590|6|Mentioned|p27|||Equivalent to Hanson Plain Sand||||||
25261|Moorabool Viaduct Sand|50078|5|Briefly described|p36, p38|||Of the Brighton Group. See also Moorabool Viaduct Sands.||||||
25261|Moorabool Viaduct Sand|50154|6|Mentioned|p136|||Geological Province: Otway Basin||||||
25261|Moorabool Viaduct Sand|60451|5|Briefly described|p95 Fig. 61|||||||||
25261|Moorabool Viaduct Sand|60581|5|Briefly described|Map Legend|Pliocene|Miocene|Silt to coarse quartz sand in quartzose-calcareous silt matrix, well sorted and rounded, moderately bedded; in parts kaolinisesd but generally ferruginised.||||||20-JAN-05
25261|Moorabool Viaduct Sand|60582|5|Briefly described|Map Legend|Pliocene|Miocene|Silt to coarse quartz sand in quartzose-calcareous silt matrix, well sorted and rounded, moderately bedded; in parts kaolinisesd but generally ferruginised.||||||20-JAN-05
25261|Moorabool Viaduct Sand|60583|5|Briefly described|Map Legend|Pliocene|Miocene|Silt to coarse quartz sand in quartzose-calcareous silt matrix, well sorted and rounded, moderately bedded; in parts kaolinisesd but generally ferruginised.||||||20-JAN-05
25261|Moorabool Viaduct Sand|60584|5|Briefly described|Map Legend|Pliocene|Miocene|Silt to coarse quartz sand in quartzose-calcareous silt matrix, well sorted and rounded, moderately bedded; in parts kaolinisesd but generally ferruginised.||||||20-JAN-05
25261|Moorabool Viaduct Sand|60585|4|Described|p32|Early Pliocene|Late Miocene|Disconformably overlies the White Hills Gravel and Calivil Formation. Grades laterally into the Hanson Plain Sand. Interfingers with the Newer Volcanics. Thickness: 10-30m. Ranges from quartzose calcareous sandy clay to coarse grained quartz sandstone.||||||
25261|Moorabool Viaduct Sand|61182|5|Briefly described|p30|||Defined by Bowler (1963). Pliocene deposits overlying the Port Campbell Limestone and older strata are regarded here as distinct from the 'Moorabool Viaduct Formation' (the Moorabool Viaduct Sand of Bowler), so are called the Hanson Plain Sand in this area..||||||10-FEB-15
25261|Moorabool Viaduct Sand|65715|5|Briefly described|p14, p16-7, p75|||Superseded name for Black Rock Sandstone. Type section near the western Batesford Quarry.||||||
25261|Moorabool Viaduct Sand|66002|6|Mentioned|p12, p13 Tb.9|||Misspelling of Moorabool Viaduct Formation? Junior synonym of Black Rock Sandstone||||||
25261|Moorabool Viaduct Sand|66012|4|Described|p4, p6, p10 Tb.1, p17-19, p27|Pliocene|Miocene|Unconformably overlies Lismore Granodiorite. Interfingers with Newer Volcanic Group. Indistinguishable from White Hills Gravel. Sands, silts and limestone. Variable thickness up to 50m thick. Lateritic weathering profile. Late Miocene to early Pliocene. [Probably Hanson Plain Sand or just Brighton Group in this area now, CEB2015].| | | | | |16-FEB-15
25261|Moorabool Viaduct Sand|68360|6|Mentioned|p225 Fig.4|||||||Shown as overlain by Beaumaris Sandstone and underlain by Fyansford Formation.||07-FEB-18
25261|Moorabool Viaduct Sand|69297|6|Mentioned|p98|Pliocene|Pliocene|||||Unconformably overlies the Puebla Formation. Unconformably overlain by the Wannaeue Formation. |Sand. |
12283|Moore formation|41993|6|Mentioned|Fig.8 P14|||||||||
38769|Mossey Creek Group|23837|6|Mentioned|p440 Fig.2|||||||||
12431|Motten Spilite""|31475|6|Mentioned|p81|||||||||
12432|Motton Spilite greenstones|37409|6|Mentioned|p177|||||||||
73427|Motton Spilite""|63168|5|Briefly described|p53, p57|||Informal name. Geological province: Fossey Mountain Trough. Correlated with Crimson Creek Formation, petrographically. Basalt lavas.||||||
77502|Motton metabasalt|61412|6|Mentioned|p9.|||See Motton Spilite.||||||
12519|Mount Bischoff Complex|31669|6|Mentioned|p72|||Used informally?||||||23-MAR-05
12520|Mount Bischoff Dolomite|41486|5|Briefly described|p630|||||||||
12520|Mount Bischoff Dolomite|41803|6|Mentioned|Fig.9|||||||||
12520|Mount Bischoff Dolomite|42178|6|Mentioned|Fig.4 P229|||||||||
12521|Mount Bischoff Series|31174|4|Described|p176|||Refers Reid (1923). Now Mt. Bischoff sequence.||||||
12523|Mount Bischoff dolomite|41803|6|Mentioned|Table 1|||||||||
38053|Mount Black Dacite|23402|5|Briefly described|p18|Late Cambrian|Late Cambrian|Of the Central Volcanic Complex.   Age: 495+/-9Ma (Ar-Ar and U-Pb zircon SHRIMP)||||||24-SEP-07
81368|Mount Black Formation|70274|4|Described|p448,451-453,455,461-464|Cambrian|Cambrian|Lithostratigraphic unit of the northern Central Volcanic Complex. Associated with felsic magmatism ~507-505 Ma and characterised by coherent and volcaniclastic rocks. Zircon analysis of massive feldspar-hornblende-phyric dacites gave a weighted average 206Pb/238U age of 504.9+\-1.0 Ma and 506.8+\-1.0 Ma, which are considered to be the crystallization ages of the different dacite samples. Also contains 1.03 Ga inherited zircon ages, interpreted to be derived from (presumably) underlying Tyennan basement.|~507-505 Ma|Unit of Mount Read Volcanics.||Overlain by Hercules and Kershaw pumice formations.|Lavas, domes, cryptodomes, and synvolcanic sills.|
40326|Mount Black dacite|23942|6|Mentioned|p965 Fig. 11|||Mount is Mt. in text.||||||
40326|Mount Black dacite|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Central Mount Read Volcanics, with U-Pb SHRIMP zircon age of 494.9+\-8.6 Ma.|494.9+\-8.6 Ma|||||
12526|Mount Black volcanics|23946|6|Mentioned|p1055|||Informal - see Mount Black Volcanics||||||
12526|Mount Black volcanics|33218|6|Mentioned|Fig.3|||||||||
12526|Mount Black volcanics|37044|6|Mentioned|Fig.8|||||||||
12526|Mount Black volcanics|41336|6|Mentioned|Fig.1|||||||||
12578|Mount Chappel Island granite|36374|4|Described|p61|||||||||
74579|Mount Cygnet measures""|63868|6|Mentioned|p17|||Informal term used by Thureau (1881) in the first significant report on the Cygnet Coal Measures. Mount is Mt in text.||||||07-FEB-11
12681|Mount Elephant Coal Horizon|41766|6|Mentioned|p25|||||||||
79563|Mount Field Member|69875|5|Briefly described|p243 Fig 5.2|Early Ordovician|Early Ordovician|Fossil control. Appears also as Mt Field Member.||Florentine Valley Formation||Underlies Karmberg Limestone. Overlies Pontoon Hill Member.||
12709|Mount Field Siltstone|40136|6|Mentioned|p24|||||||||
12817|Mount Inglis Sandstone|23837|6|Mentioned|p440 Fig.2|||||||||
12817|Mount Inglis Sandstone|30155|6|Mentioned|Fig.33.4|||||||||
12817|Mount Inglis Sandstone|36817|4|Described|p62|||Type section given on P55.||||||
81369|Mount Jukes rhyodacite|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Central Mount Read Volcanics, with U-Pb SHRIMP zircon age of 503.3+\-13.8 Ma.|503.3+\-13.8 Ma|||||
40508|Mount Julia Members|23947|6|Mentioned|p1078|||Misspelt - see Mount Julia Member.||||||24-SEP-07
23822|Mount Kerford granite|36374|3|Fully described|p52|||||||||
23822|Mount Kerford granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
12879|Mount La Perouse Formation""|42349|5|Briefly described|Fig.3 P64|||||||||
12903|Mount Mackenzie Conglomerate|37412|6|Mentioned|p28|||||||||
25286|Mount Mackenzie Sandstone and Conglomerate|37412|2|Defined|p24|Proterozoic|Proterozoic|Prob. Proterozoic||||||
25286|Mount Mackenzie Sandstone and Conglomerate|69874|5|Briefly described|p174|Cambrian|Cambrian|600m thick.||Clytie Cove Group.||Overlies Mount Rugby Conglomerate. Is overlain by Long Bay Shale.|Interbedded sandstone and pebble conglomerate in the lower part, passing upwards into mainly interbedded sandstone and siltstone, with common graded bedding.|
32861|Mount Nicholas Beds|48846|14|Not recorded|p9,25|||||||||
33480|Mount Paris Alkali-Feldspar Granite|63171|5|Briefly described|p260, p472, p475||Devonian|Alkali-feldspar body with sheet-like form  is very similar to the Lottah pluton. In the Blue Tier batholith.||||||
13009|Mount Paris granite|37797|6|Mentioned|p139|||||||||
33455|Mount Pearson Adamellite|63171|5|Briefly described|p257, 259|||One of the main adamellites in the Blue Tier batholith. Compositionally similar to Poimena Adamellite but is very coarse-grained biotite adamellite, with abundant K-feldspar megacrysts||||||
13015|Mount Pearson adamellite|39927|6|Mentioned|p305|||||||||
13016|Mount Pearson granite|37797|6|Mentioned|p141|||||||||
13016|Mount Pearson granite|67503|6|Mentioned|p54|||Informal.||||||
13032|Mount Pierson Adamellite|35826|3|Fully described|p130|||||||||
69942|Mount Read - Stavely Volcanics|60904|6|Mentioned|p806 Fig. 25d|||Composite term for the Mount Read and Mount Stavely Volcanics - not intended as a formal name. See also p807 Fig. 25e.||||||
37820|Mount Read Volcanic Complex|24214|6|Mentioned|p788|||Mount is Mt. in text.||||||
37820|Mount Read Volcanic Complex|60412|6|Mentioned|p242, 246|Cambrian|Cambrian|Tasmania. Crystallisation age is coeval with that of the metavolcanic rocks at Mount Stavely (VIC).|c.500 Ma.|||||
37820|Mount Read Volcanic Complex|64616|6|Mentioned|p326|Cambrian|Cambrian|Western Tasmania. Geochemistry and age are similar to those of the Cambrian grenstones on the E margin of the Melbourne Zone, suggesting continuity of basement rocks across Bass Strait.||||||
13054|Mount Read Volcanic Formation|39780|6|Mentioned|p1|||||||||
13055|Mount Read Volcanic Group|29914|6|Mentioned|Fig.1|||||||||
13055|Mount Read Volcanic Group|29930|6|Mentioned|p1086|||||||||
13055|Mount Read Volcanic Group|30032|6|Mentioned|Fig.1|||||||||
13056|Mount Read Volcanics complex|30212|6|Mentioned|p28|||||||||
73804|Mount Read Volcanics""|638|5|Briefly described|p86|||Informal - see Mount Read Volcanics. Of Campana and King (1963). Also referred to as the "porphyroids" in earlier studies. ||||||
40424|Mount Read volcanic complex|24576|6|Mentioned|p726 Fig. 1|||Mount is Mt. in text.||||||
40424|Mount Read volcanic complex|60904|6|Mentioned|p803|||Informal name. Mount is Mt in text.||||||
13058|Mount Read volcanics|23215|5|Briefly described|p123||Cambrian|Written: Mt Read volcanics. Age: 515-550 Ma.||||||
13058|Mount Read volcanics|31765|5|Briefly described|p31|||||||||
13058|Mount Read volcanics|40074|6|Mentioned|p176|||||||||
13058|Mount Read volcanics|73430|6|Mentioned|p491|Late Cambrian|Late Cambrian|See also Mount Read Volcanics p512, p518. [Written as Mt Read volcanics.]|||||Largely felsic to intermediate composition.|
70024|Mount Read-Stavely Volcanics|60904|6|Mentioned|p806 Fig. 25d|||Composite term for the Mount Read and Mount Stavely Volcanics - not intended as a formal name. See also p807 Fig. 25e.||||||
30102|Mount Reed Volcanics|23718|5|Briefly described|p18|||||||||
30102|Mount Reed Volcanics|43093|5|Briefly described|p13|||Misspelling of Mount Read Volcanics.||||||
31759|Mount Reid Volcanics (TAS)|43834|6|Mentioned|p29||Cambrian|Misspelling of Mount Read Volcanics.||||||
13061|Mount Reid volcanics|41856|6|Mentioned|p382|||||||||
13061|Mount Reid volcanics|50591|6|Mentioned|p5.1|Paleoproterozoic|Paleoproterozoic|Age: 1847 +/- 16Ma.||||||07-NOV-08
81328|Mount Roland Conglomerate|70025|4|Described|p4-5|Late Ordovician|Cambrian|Tyennan Zone. Abbreviated as MR on p4 Fig 2. Present along north coast of Tasmania alongside tectonic melange and mafic-ultramafic complex rocks, overlying Cambrian chert (Seymour and Vicary 2010; Everard and Calver 2014).|||||Conglomerate, sandstone.|
30499|Mount Stewart Complex|43191|6|Mentioned|p46|||Contains ultramafic associations.||||||
73428|Mount Stewart complex|63168|6|Mentioned|p72|||Informal name. Mount is Mt in text. ||||||
73428|Mount Stewart complex|63169|5|Briefly described|p158|||Informal name. Includes layered dunite-harzburgite ultramafic associations. Geological Province: Dundas Trough.||||||31-OCT-07
33476|Mount Stronach Alkali-Feldspar Granite|63171|5|Briefly described|p257|||||||||
13120|Mount Stuart metaperidotite|41795|6|Mentioned|Fig.52B|||||||||
13209|Mount Wellington dolerite|30394|6|Mentioned|p8|||||||||
13221|Mount William adamellite|41818|6|Mentioned|p28|||||||||
13222|Mount William alkali-feldspar granite|39927|6|Mentioned|p305|||||||||
25298|Mount William biotite-muscovite granite|35825|6|Mentioned|p171|||||||||
28819|Mount William granites|35825|6|Mentioned|p171|||||||||
13224|Mount William medium-grained biotite-mus|35824|6|Mentioned|Map legend|Devonian|Devonian|||||||
13257|Mount Zeehan Conglomerate""|42204|6|Mentioned|p233|||||||||
73289|Mount Zeehan conglomerate sequence|63238|6|Mentioned|p22|||Informal name. ||||||
80019|Mourum Member|69297|5|Briefly described|p79|Coniacian|Turonian|Otway Basin. ||Belfast Mudstone||Overlies the Flaxman Formation. Overlain by the Mount Salt Formation. |Mudstone and siltstone. |
13490|Munro Creek Formation|37045|6|Mentioned|p221|||||||||
73268|Munro Creek Slate and Quartzite""|63240|5|Briefly described|p4|||Redesignated from "Rosebery Group" to marine Owen Group from fossil evidence and lithology.||||||14-MAY-07
13497|Murchison Gorge Volcanics|40890|6|Mentioned|Fig.2|||||||||
13499|Murchison River Granite|33839|6|Mentioned|Fig.3|||||||||
13499|Murchison River Granite|68314|6|Mentioned|p755 Fig.6|Middle Cambrian|Middle Cambrian|Age inferred from Fig.6.|501 +/- 6 Ma (Perkins and Walshe, 1993).|||||
13499|Murchison River Granite|73369|4|Described|p295, 307, 313, 322|||K-Ar age 515+/-15 m.y.|||||Adamellite.|
13500|Murchison River granite|30278|6|Mentioned|p184|||||||||
40335|Murchison granite|23940|6|Mentioned|p915|||||||||
40335|Murchison granite|24290|6|Mentioned|p910|||Informal name.||||||
40335|Murchison granite|63169|6|Mentioned|p161|||||||||
40335|Murchison granite|70274|4|Described|p445,447-448,450,455,460-462,465|Cambrian|Cambrian|Granitic body found within the central Mount Read Volcanics, with Ar-Ar hornblende age of 501.5+\-11.4 Ma. Intrudes Western Volcano-Sedimentary Sequences, Central Volcanic Complex, and Eastern Quartz-Phyric Sequence. Potentially coeval with Mount Cripps Subgroup ignimbrites? Interpreted as subvolcanic intrusions genetically related to the host volcanic successions (Large et al., 1996), and may have played important roles in driving hydrothermal circulation that formed VHMS deposits in the belt (Large et al., 1996; Huston et al., 2011). Zircon analysis yields a weighted average 206Pb/238U age of 497.3+\-0.9 Ma.|497+\-0.9 Ma|||Overlain locally by (upper?) Tyndall Group.|Medium-grained quartz + K-feldspar + plagioclase + biotite + hornblende+\-apatite+\-zircon+\-rutile granite or granodiorite.|
13612|Mussel Roe Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on informal Musselroe Point microgranite.||||||
31638|Mussel Roe Suite|42726|5|Briefly described|map legend||Middle Devonian|||||||
73637|Musselroe Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Musselroe Suite, Eddystone Batholith.  S-type granite, felsic, weakly fractionated, reduced. Name implied from map legend.||||||
73637|Musselroe Granite|69876|5|Briefly described|p306 Tb 6.1|Devonian|Devonian|Shown as unit in Boobyalla Suite [currently (2016) in Musselroe Suite]. Age inferred.|||||S-type granite.|
73637|Musselroe Granite|71730|6|Mentioned|p33, p35, p37, p43, p57|||Chemically and petrogrpahically resembles the Ansons Bay Granite.|||||Poorly defined coarse-grained granitre.|
73638|Musselroe Point Granite|61216|5|Briefly described|p21|||Presented only as Musselroe Point in text. Adamellite/granite pluton containing biotite and minor amounts of garnet and/or cordierite. S-type granite.||||||10-FEB-11
73638|Musselroe Point Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Musselroe Suite, Eddystone Batholith.  S-type granite, felsic, weakly fractionated, reduced. Name implied from map legend.||||||
73638|Musselroe Point Granite|69876|5|Briefly described|p306 Tb 6.1|Devonian|Devonian|Shown as unit in Boobyalla Suite [currently (2016) in Musselroe Suite]. Age inferred. Also Musselroe Point body, pluton.|||||S-type adamellite/granite containing biotite and minor amounts of garnet and/or cordierite.|
28838|Musselroe Point microgranite|35824|6|Mentioned|Map legend|Devonian|Devonian|||||||
28838|Musselroe Point microgranite|35825|4|Described|p165|||||||||
40881|Musselroe Suite|61216|6|Mentioned|p24, p29|||Shows linear trend of granites.||||||10-FEB-11
40881|Musselroe Suite|65646|6|Mentioned|p17, p20.|||S-type. Contains peraluminous granites. Probably substantially restite-fractionated.||||||08-FEB-16
13619|Mutton Spilite|42891|6|Mentioned|p298|||misspelling of Motton Spilite||||||
23866|Narrows Sandstone and Conglomerate|37412|2|Defined|p26|Proterozoic|Proterozoic|Prob. Proterozoic||||||
23866|Narrows Sandstone and Conglomerate|69874|5|Briefly described|p174|Cambrian|Cambrian|200m thick.||Clytie Cove Group.||Overlies Long Bay Shale. Is overlain by Joan Point Sandstone.||
13913|Narrows Sandstone and conglomerate|37412|6|Mentioned|p26|||||||||
13926|Nassau Siltstone|23837|6|Mentioned|p440 Fig.2|||||||||
13926|Nassau Siltstone|24552|4|Described|p5 Fig.2, p8|Artinskian|Sakmarian|Fossiliferous (bryozoans, described, and brachiopods) grey-black siltstone. Overlies Faulkner Group, overlain by Berriedale Limestone. Of Cascades Group. Geological Province: Tasmanian Basin.||||||24-DEC-15
13926|Nassau Siltstone|30153|6|Mentioned|p152|||Base of Cascades Group. Fauna.||||||
13926|Nassau Siltstone|30155|6|Mentioned|Fig.33.4|||||||||
13926|Nassau Siltstone|31780|5|Briefly described|p12|||||||||
13926|Nassau Siltstone|32945|6|Mentioned|p85|||Permian. See also P86.||||||
13926|Nassau Siltstone|33494|6|Mentioned|p45|||||||||
13926|Nassau Siltstone|33711|6|Mentioned|Table 1|||||||||
13926|Nassau Siltstone|34099|6|Mentioned|Fig.1|||Perm. Cascades Gp.||||||
13926|Nassau Siltstone|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
13926|Nassau Siltstone|35284|6|Mentioned|Fig.1|||||||||
13926|Nassau Siltstone|36207|6|Mentioned|Text Fig.2|||||||||
13926|Nassau Siltstone|37477|6|Mentioned|Fig.2|||||||||
13926|Nassau Siltstone|38196|6|Mentioned|p682|||||||||
13926|Nassau Siltstone|38197|5|Briefly described|p683|||||||||
13926|Nassau Siltstone|38505|6|Mentioned|Fig.2|||||||||
13926|Nassau Siltstone|38610|6|Mentioned|Fig.2|||||||||
13926|Nassau Siltstone|41548|6|Mentioned|Fig.1|||||||||
13926|Nassau Siltstone|41895|6|Mentioned|p28|||||||||
13926|Nassau Siltstone|42381|5|Briefly described|Fig.1 P84|||||||||
13926|Nassau Siltstone|43474|14|Not recorded|p7||Sakmarian|||||||
13926|Nassau Siltstone|65645|5|Briefly described|p27 Appendix|Permian|Permian|Age: Bernacchian Stage.|||||Fossiliferous siltstone and calcareous siltstone.|24-DEC-15
13926|Nassau Siltstone|65647|5|Briefly described|Appendix p10|Artinskian|Sakmarian|Of lower Parmeener Supergroup. 36 m thick. Fossiliferous siltstone and calcareous siltstone. Bernacchian Stage age.||||||
13926|Nassau Siltstone|65662|5|Briefly described|p10. |||||Unit in Lower Parmeener Supergroup.||Overlies Rayner Sandstone. Is overlain by Berriedale Limestone.|Fossiliferous siltstone, calcareous siltstone.|
13926|Nassau Siltstone|66174|14|Not recorded|?|||||||||
13926|Nassau Siltstone|67501|6|Mentioned|p7, Fig.8 p17,|||||Parmeener Supergroup (Lower)||Overlies Faulkner Group; is overlain by Minnie Point Formation.|Richly fossiliferous, dark grey, glaciomarine siltstone, calcareous siltstone and sandstone.|
13926|Nassau Siltstone|69877|5|Briefly described|p371|Permian|Permian|Hobart region. 30m thick. Similar facies occur on Maria Island (Skipping Ridge Formation). Early Bernacchian age. See also reference to Nassau Formation (p373 Fig.7.15).||Unit in Cascades Group.|||Calcareous fossiliferous (abundant brachiopods and bryozoans), marine grey-black siltstone.|
13926|Nassau Siltstone|73321|6|Mentioned|Map legend|Permian|Permian|Correlates of Nassau Siltstone are included in a map unit described as dominantly richly fossiliferous, interbedded glaciomarine grey bioclastic and argillaceous limestone and calcareous siltstone; lower beds of fossiliferous siltstone; in part contact metamorphosed by dolerite.||Lower Parmeener Supergroup||||
13926|Nassau Siltstone|73322|5|Briefly described|Map legend|Permian|Permian|Grouped in a map unit with Rayner Sandstone, described together as dark grey, fossiliferous siltstone and calcareous siltstone, and basal pebbly sandstone.||Cascades Group|||Dark grey, fossiliferous siltstone and calcareous siltstone.|
13926|Nassau Siltstone|73323|6|Mentioned|Map legend|Permian|Permian|Included with Berridale Limestone and Rayner Sandstone in map unit described as dominantly richly fossiliferous, interbedded glaciomarine grey bioclastic and argillaceous limestone, calcareous siltstone and rare metabentonite layers, overlying dark grey fossiliferous siltstone and calcareous siltstone and basal fossiliferous poorly-sorted pebbly sandstone.||Lower Parmeener Supergroup||||
13926|Nassau Siltstone|73324|5|Briefly described|Map legend|Permian|Permian||||||Dark grey richly- to sparsely-fossiliferous siltstone and calcareous siltstone.|
13926|Nassau Siltstone|73327|5|Briefly described|Map legend|Permian|Permian|Map unit also includes Berridale Limestone and Rayner Sandstone with collective description of dominantly richly fossiliferous, interbedded glaciomarine grey bioclastic and argillaceous limestone and calcareous siltstone; lower beds of fossiliferous siltstone; basal pebbly sandstone bed in northern areas; in part contact metamorphosed by dolerite.||Lower Parmeener Supergroup|||Fossiliferous siltstone. In part contact metamorphosed by dolerite.|
30663|Neasey Beds|43336|14|Not recorded|p23|||||||||
78557|Neasey Quartzites and Slates|67502|6|Mentioned|p31|||McNeil, 1961; Matthews, 1961; Longman and Matthews, 1962; Nye et al. 1934. Name considered redundant: rocks now included in the Cowrie Siltstone.||||||
78557|Neasey Quartzites and Slates|69873|6|Mentioned|p43|||Superseded by Cowrie Siltstone.||||||
73354|Neasy Quartzites and Slates|63167|5|Briefly described|p14|Precambrian|Precambrian|As well as quartz, also contain slate, phyllite and quartz phyllite.Originally incorporated rocks of the Detention Subgroup and Jacob Quartzite.||||||
29302|Nelson Formation (TAS)|42425|5|Briefly described|Table 2 P140, P147|||Compare with Nelson Formation, SA & Vic. Is State wrong? Invalidly reserved for Tas.||||||
14065|New River Beds|37408|4|Described|p96|||Reserved as New River Lagoon||||||
14065|New River Beds|63263|5|Briefly described|p61|Middle Ordovician|Middle Ordovician|Calcarenitic platform-margin facies.||||||07-FEB-11
14065|New River Beds|69875|5|Briefly described|p254|||Burrett et al. (1981). 130m thick. Fauna described.||||Underlies Precipitous Bluff Beds.|Thick-bedded, richly fossiliferous calcarenite and micrite; Calathium and corals comprising reef facies in upper part of formation; reworked bryozoans, echinoderms and calcareous algae common.|
39917|New Town Formation|24549|5|Briefly described|Map 4686|Triassic|Triassic|Max Thickness: 435ft. Name used interchangeably with Newtown Formation in Strat. Table notes (Map 4785), Weston Creek area.||||||
14102|Newer granite|33354|5|Briefly described|p182|||Age. Refers McDougall & Leggo (1965).||||||
83424|Newton Creek Formation|69842|6|Mentioned|p9|||Trial map; correlated with fossiliferous siltstone and greywacke at 358 200 mE, 5 355 750 mN.||Owen Group.||||
28865|Newton Creek Sandstone Member|638|5|Briefly described|p88 Fig. 4.2|Late Cambrian|Late Cambrian|Of the Owen Conglomerate (Gordon Group).  ||||||
28865|Newton Creek Sandstone Member|33738|6|Mentioned|p45|||||||||
28865|Newton Creek Sandstone Member|36054|6|Mentioned|p437|||||||||
28865|Newton Creek Sandstone Member|39892|6|Mentioned|p29|||||||||
28865|Newton Creek Sandstone Member|40070|6|Mentioned|p17|||||||||
28865|Newton Creek Sandstone Member|40890|6|Mentioned|Fig.3|||||||||
28865|Newton Creek Sandstone Member|41143|6|Mentioned|p272|||||||||
28865|Newton Creek Sandstone Member|41896|6|Mentioned|p16|||||||||
28865|Newton Creek Sandstone Member|42976|5|Briefly described|p267|||Of Owen Conglomerate.||||||30-JUN-08
28865|Newton Creek Sandstone Member|43241|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
28865|Newton Creek Sandstone Member|43242|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Spelt out as Newton Creek Sandstone (Member).||||||30-JUN-08
28865|Newton Creek Sandstone Member|43243|5|Briefly described|Map Legend|Ordovician|Cambrian|Spelt out as Newton Creek Sandstone (Member).||||||30-JUN-08
28865|Newton Creek Sandstone Member|43777|5|Briefly described|p4|Iverian|Idamean|||||||
28865|Newton Creek Sandstone Member|63168|5|Briefly described|p75 Fig. 3.10|Late Cambrian|Late Cambrian|In Queenstown, Tyndall Range area. ||||||
28865|Newton Creek Sandstone Member|63170|5|Briefly described|p189, p190|||Of the Owen Conglomerate. Comprises quartzwacke, bioturbated thin-bedded sandstone, micaceous siltstone and grey siliceous conglomerate. Fossil fragments contained.||||||07-FEB-11
14115|Newton Creek Sandstone Member""|30276|6|Mentioned|p19|||See also P20||||||
40509|Newton Creek dacites|23947|5|Briefly described|p1075|||Of the Central Volcanic Complex||||||
83233|Newtown Coal Measures|73322|6|Mentioned|Map legend|Triassic|Triassic|Included as part of a map unit described as interbedded cross-bedded white quartzose sandstone, quartz-rich lithic sandstone, siltstone and mudstone||Upper Parmeener Supergroup||||
83233|Newtown Coal Measures|73323|6|Mentioned|Map legend|Triassic|Triassic|Included in a map unit of thick- to thin-bedded volcanic lithic sandstone, siltstone, mudstone and coal seams, fossil plants; and an additional map unit of interbedded cross-bedded white quartzose sandstone, quartz-rich lithic sandstone, siltstone and mudstone; upper interval with much dark grey carbonaceous mudstone, thin lenticular coal seams and fossil plants in places.||Upper Parmeener Supergroup||||
83233|Newtown Coal Measures|73324|5|Briefly described|Map legend|Triassic|Triassic||||||Thick- to thin-bedded volcanic lithic sandstone, siltstone, mudstone and coal seams, fossil plants on some horizons.|
83233|Newtown Coal Measures|73326|6|Mentioned|Map legend|Triassic|Triassic|Included in a map unit of thick- to thin-bedded volcanic lithic sandstone, siltstone, mudstone and coal seams with fossil plants; and an additional map unit of interbedded cross-bedded white quartzose sandstone, quartz-rich lithic sandstone, siltstone and mudstone; upper interval with common dark grey carbonaceous mudstone, occasional thin lenticular coal seams and fossil plants in places.||Upper Parmeener Supergroup||||
83233|Newtown Coal Measures|73328|6|Mentioned|Map legend|Triassic|Triassic|Map unit contains Newton Coal Measures in part, described as thick- to thin-bedded volcanic lithic sandstone, siltstone, mudstone and coal seams, fossil plants on some horizons. Also included in an additional map unit of interbedded cross-bedded white quatrzose sandstone, quartz-rich lithic sandstone, siltstone and mudstone; upper interval with much dark grey carbonaceous mudstone, thin lenticular coal seams and fossil plants in places.||Upper Parmeener Supergroup||||
77850|Newtown Formation (TAS)|24549|6|Mentioned|Map 4785|||Max Thickness: 435ft. Name used interchangeably with New Town Formation in Strat. Table notes (Map 4785), Weston Creek area.||||||
73430|Nineteen Mile Creek Dunite|63168|6|Mentioned|p71|||Of Rubenach (1973). ||||||
73430|Nineteen Mile Creek Dunite|69874|4|Described|p111 Fig4.12,p123 Fi 4.21,p128-130,p143|Middle Cambrian|Early Cambrian|See also. Up to 1.3 km thick. Associated with osmiridium deposits. The PGE crystallised from boninitic magmas before being emplaced into crustal magma chambers. Cr/Mg diagram.||Basal Heazlewood River Complex.||Overlain by Purcells Plain Lherzolite and in the E by Fentons Spur Peridotite.|Strongly deformed adcumulate sequence of massive, partly (50-60%) serpentinized dunite with subordinate thin (10-1000mm) layers of harzburgite and orthopyroxenite; highly magnesian olivine and orthopyroxene, with accessory chrome spinel.|
14163|Nineteen Mile Creek dunite|37056|6|Mentioned|Fig.1|||||||||
40216|Nirranda group|24200|5|Briefly described|p408|Oligocene|Eocene|Informal - see Nirranda Group.  Geological Province: Otway basin.||||||
40216|Nirranda group|24551|6|Mentioned|p248 Fig. 9.11|||||||||
40216|Nirranda group|24562|5|Briefly described|p3, 7, Table 1|||Geological Province: Otway Basin.||||||
40216|Nirranda group|50154|6|Mentioned|p132|Miocene|Paleocene|Geological Province: Otway Basin.||||||16-SEP-04
34488|No.1 dolomite|22770|5|Briefly described|Fig3 p769,769|||Informal subdivision of Crimson Creek Formation (misspelt as Crimson Creek Group in Fig. 3) in Renison mine area.||||||10-APR-07
34488|No.1 dolomite|64394|5|Briefly described|p98|||Conformable on Red Rock Member. Thickness: 8-25m. A chemically impure equivalent of No. 2 + No. 3 Dolomites, having well-dev'd silt-mudstone interbeds up to 4m thick. Carbonate unit, stromatolitic-oolite facies - hosting stratabound mineralisation.||||||05-NOV-08
34487|No.2 dolomite|22770|5|Briefly described|Fig3p769,769||Proterozoic|Informal subdivision of Success Creek Group in Renision mine area.||||||
34487|No.2 dolomite|64394|5|Briefly described|p98|||Overlain by Red Rock Member. Carbonate unit, stromatolitic-oolite facies - hosting stratabound mineralisation.||||||05-NOV-08
34486|No.3 dolomite|22770|5|Briefly described|Fig3p769,769||Proterozoic|Informal subdivision of Success Creek Group in Renision mine area.||||||
34486|No.3 dolomite|64394|5|Briefly described|p98|||This is the lowermost of the three carbonate units which host stratabound mineralisation. Max. thickness: 15m. Carbonate unit, stromatolitic-oolite facies.||||||
73283|Noddy Creek Volcanics""|63240|5|Briefly described|p6|||Extensive volcano-sedimentary and sedimentary sequences with andesitic to felsic rocks. Assigned to the Western Volcano-Sedimentary Sequence.||||||
73283|Noddy Creek Volcanics""|67654|6|Mentioned|p80|||See also Noddy Creek Volcanics.||||||
14202|Noddy Creek lamprophyre|33354|6|Mentioned|p183|||Petrology.||||||
81370|Noddy Creek volcanics|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Tyndall Group, with U-Pb SHRIMP zircon age of 502.8+\-8.8 Ma.|502.8+\-8.8 Ma|||||
42038|Nora formation|50091|5|Briefly described|p408 Fig.1|Ordovician|Ordovician|Conodonts found.  Geological Province: Georgina Basin.||||||04-NOV-04
79498|North Heemskirk Gabbro|69874|5|Briefly described|p139, p119 Table 4.2, p120 Fig 4.18|||North of Heemskirk Granite. Likened to low-Ti McIvor Hill Complex, but major analysis is ferrogabbro with 2.96% TiO2.|||||Gabbro; coarse-grained uralitised augite-labradorite gabbro.|
83309|North Lyell Chert|73170|5|Briefly described|p794|Cambrian|Cambrian|In the North Lyell ""Corridor Zone"" group of deposits in the Mount Lyell mine area. 700m long, 100m wide, 500m down dip. The author states reluctance to use the lithological term ""chert"".|||||An intensely silicified body of cryptocrystalline quartz; an alteration lithology. Has associated bornite mineralisation.|
73431|Nubeena Quartzite|63168|6|Mentioned|p50 Tb. 3.1|||name probably obsolete - incorporated into the Oonah Formation.||||||
14324|Nubeena Quartzite""|41795|6|Mentioned|p12|||||||||
14450|O'Brien Formation|39717|6|Mentioned|p644|||Misspelling of O'Briens. Crimson Ck.Fm.has precedence.||||||
14451|O'Briens Formation|39361|6|Mentioned|p1441|||Crimson Ck.Fm. has precedence over this name.||||||
73138|Ocean Floor Basalt|44135|6|Mentioned|p15|||||||||07-DEC-09
73138|Ocean Floor Basalt|63168|6|Mentioned|p47, p64, p68|||Probably not a formal name - indicates a type of basalt as does Within Plate Basalt. ||||||
73139|Ocean-Floor Basalt suite|44135|6|Mentioned|p15|||Informal reference to Ocean Floor Basalt.||||||07-DEC-09
14604|Oonah Quartzite|31264|6|Mentioned|p838|||||||||
14604|Oonah Quartzite|31832|6|Mentioned|p53|||||||||
14604|Oonah Quartzite|33839|6|Mentioned|p568|||||||||
14604|Oonah Quartzite|41795|5|Briefly described|p12|||||||||
28893|Oonah Quartzite and Slate|30281|6|Mentioned|p6|||||||||
28893|Oonah Quartzite and Slate|31141|4|Described|p3|||||||||
28893|Oonah Quartzite and Slate|31174|6|Mentioned|p174|||Refers Spry (1958)||||||
28893|Oonah Quartzite and Slate|31648|6|Mentioned|p133|||See also Fig. 2 & P40.||||||
28893|Oonah Quartzite and Slate|33853|6|Mentioned|Fig.1|||Prot. - Camb.||||||
28893|Oonah Quartzite and Slate|35670|4|Described|p16|||Stratigraphy discussed on P19||||||
28893|Oonah Quartzite and Slate|40070|4|Described|p8|||||||||
28893|Oonah Quartzite and Slate|41795|6|Mentioned|p12|||||||||
28893|Oonah Quartzite and Slate|63168|5|Briefly described|p50 Tb. 3.1|||Of Blissett (1962b). Incorporated into the Oonah Formation. ||||||
14605|Oonah Slate|31264|6|Mentioned|p838|||||||||
14606|Oonah formation|35670|6|Mentioned|p19|||||||||
14606|Oonah formation|42178|6|Mentioned|p225|||||||||
14606|Oonah formation|63167|5|Briefly described|p19|||Informal - see Oonah Formation. ||||||
14697|Overflow Formation|42416|6|Mentioned|p193|||Variation of Overflow Creek Formation?||||||
27530|Owen Conglomerate|638|5|Briefly described|p84, p85 Fig. 4.1|Early Ordovician|Late Cambrian|Of the Denison Group.Subdivided into the Upper, Middle and Lower Owen based on varied lithologies (details included in Tb. 4.3, p125).  Overlies Tyndall Group rocks in places.  Unclear how Owen Conglomerate relates to Owen Formation? See also p104.||||||
27530|Owen Conglomerate|22551|6|Mentioned|p148|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|23113|5|Briefly described|p475|||||||||
27530|Owen Conglomerate|23923|5|Briefly described|p1216, 1217, 1218 Fig. 3|Early Devonian|Ordovician|Of the Denison Group.  Overlain by Moina Sandstone.||||||17-JAN-07
27530|Owen Conglomerate|23940|6|Mentioned|p916 Fig. 2|||||||||
27530|Owen Conglomerate|23947|5|Briefly described|p1074, p1076|Early Ordovician|Late Cambrian|Overlies the Zig Zag Hill Formation.||||||
27530|Owen Conglomerate|23949|6|Mentioned|p1129|||||||||
27530|Owen Conglomerate|24002|6|Mentioned|p233|||||||||
27530|Owen Conglomerate|24547|6|Mentioned|p20, p26|||||||||
27530|Owen Conglomerate|24548|3|Fully described|p6|Tremadocian|Tremadocian|Of the ?Junee Group. Underlain by Davey Group (unconformable). Max Thickness: ~300ft. See also Maps 4687 and 46-88.||||||04-OCT-07
27530|Owen Conglomerate|24570|5|Briefly described|p396 Fig. 5|Early Ordovician|Early Ordovician|Coarse siliciclastic molasse.||||||
27530|Owen Conglomerate|24601|3|Fully described|p835-840, p843-844, p846-851|Late Cambrian|Middle Cambrian|Subdivided into 4 informal units. Temporal equivalent of Denison Group. Age from stratigraphic relations, no older than Mount Read Volcanics. Max thickness 1400m.|</= 502 Ma.|||Conformably overlies the Tyndall Group.|Coarse-grained conglomerate, sandstone and mudstone succession.|16-MAR-12
27530|Owen Conglomerate|29585|5|Briefly described|p18|||||||||
27530|Owen Conglomerate|29875|6|Mentioned|Fig.7|||||||||
27530|Owen Conglomerate|29914|6|Mentioned|Fig.1|||||||||
27530|Owen Conglomerate|29930|6|Mentioned|p1086|||||||||
27530|Owen Conglomerate|30032|6|Mentioned|p621|||||||||
27530|Owen Conglomerate|30212|6|Mentioned|p27|||||||||
27530|Owen Conglomerate|30275|6|Mentioned|p118|||Refers Wade and Solomon(1958)||||||
27530|Owen Conglomerate|30276|6|Mentioned|p16|||||||||
27530|Owen Conglomerate|30277|6|Mentioned|p211|||Refers Carey and Banks(1954)||||||
27530|Owen Conglomerate|30278|6|Mentioned|p178|||On map. Ordovician age.||||||17-JAN-07
27530|Owen Conglomerate|30279|6|Mentioned|p122|||Part of Junee Group. Banks(1962)||||||
27530|Owen Conglomerate|30281|4|Described|p9|||||||||
27530|Owen Conglomerate|31174|6|Mentioned|Fig. 38|||Ordovician||||||
27530|Owen Conglomerate|31175|6|Mentioned|Fig. 7|||||||||
27530|Owen Conglomerate|31461|6|Mentioned|p47|||||||||
27530|Owen Conglomerate|31462|6|Mentioned|Fig.2|||Ord.-Camb.||||||
27530|Owen Conglomerate|31463|6|Mentioned|p174|||||||||
27530|Owen Conglomerate|31464|6|Mentioned|p375|||||||||
27530|Owen Conglomerate|32627|4|Described|p15, p21|Ordovician|Ordovician|Described in terms of Owen Conglomerate correlates. See also p22.||||||06-FEB-08
27530|Owen Conglomerate|32783|6|Mentioned|p1037|||||||||
27530|Owen Conglomerate|32794|6|Mentioned|p608|||||||||
27530|Owen Conglomerate|33218|6|Mentioned|Fig.2|||||||||
27530|Owen Conglomerate|33220|6|Mentioned|p4|||Ord.||||||
27530|Owen Conglomerate|33281|6|Mentioned|p11|||Mount Lyell orebody country rock.||||||17-JAN-07
27530|Owen Conglomerate|33738|6|Mentioned|p45|||||||||
27530|Owen Conglomerate|33839|4|Described|p575|||||||||
27530|Owen Conglomerate|33864|6|Mentioned|p39|||||||||
27530|Owen Conglomerate|34012|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
27530|Owen Conglomerate|34298|6|Mentioned|Fig.4|||Ord.||||||
27530|Owen Conglomerate|34501|6|Mentioned|p39|||Lower Ordovician. See also pp41,42.||||||17-JAN-07
27530|Owen Conglomerate|34502|6|Mentioned|Fig.2|||Ordovician||||||
27530|Owen Conglomerate|35092|6|Mentioned|p108|||||||||
27530|Owen Conglomerate|35118|6|Mentioned|p429|||||||||
27530|Owen Conglomerate|35153|6|Mentioned|Fig.1|||||||||
27530|Owen Conglomerate|35288|6|Mentioned|p38|||||||||
27530|Owen Conglomerate|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tasmania.||||||17-JAN-07
27530|Owen Conglomerate|35818|5|Briefly described|p6|||||||||
27530|Owen Conglomerate|35844|6|Mentioned|p10, Fig. 12|||Stratigraphy.||||||24-MAY-07
27530|Owen Conglomerate|36053|6|Mentioned|p435|||See also Fig.1.||||||
27530|Owen Conglomerate|36054|6|Mentioned|p436|||||||||
27530|Owen Conglomerate|36055|6|Mentioned|p438|||||||||
27530|Owen Conglomerate|36161|6|Mentioned|Fig.1|||||||||
27530|Owen Conglomerate|36350|6|Mentioned|Fig.1|||||||||
27530|Owen Conglomerate|36373|6|Mentioned|p37|||||||||
27530|Owen Conglomerate|36534|6|Mentioned|p226|||||||||
27530|Owen Conglomerate|36732|6|Mentioned|p297|||||||||
27530|Owen Conglomerate|36817|4|Described|p40|||See also p25.||||||17-JAN-07
27530|Owen Conglomerate|37044|6|Mentioned|p196|||||||||
27530|Owen Conglomerate|37045|6|Mentioned|p210|||||||||
27530|Owen Conglomerate|37047|6|Mentioned|p247|||||||||
27530|Owen Conglomerate|37048|6|Mentioned|p286|||||||||
27530|Owen Conglomerate|37051|6|Mentioned|p353|||||||||
27530|Owen Conglomerate|39319|6|Mentioned|p353|||||||||
27530|Owen Conglomerate|39892|5|Briefly described|p29|||||||||
27530|Owen Conglomerate|40070|6|Mentioned|p16|||||||||
27530|Owen Conglomerate|40136|5|Briefly described|p35|||||||||
27530|Owen Conglomerate|40638|6|Mentioned|p193|||||||||
27530|Owen Conglomerate|40736|6|Mentioned|p1343|||||||||
27530|Owen Conglomerate|40746|6|Mentioned|p360|||||||||
27530|Owen Conglomerate|40760|4|Described|p169|||||||||
27530|Owen Conglomerate|40890|4|Described|p47|||||||||
27530|Owen Conglomerate|41142|6|Mentioned|Fig.1|||||||||
27530|Owen Conglomerate|41143|5|Briefly described|p272|||||||||
27530|Owen Conglomerate|41148|6|Mentioned|p1241|||||||||
27530|Owen Conglomerate|41317|3|Fully described|p175|||||||||
27530|Owen Conglomerate|41488|6|Mentioned|p28|||||||||
27530|Owen Conglomerate|41570|6|Mentioned|p101|||||||||
27530|Owen Conglomerate|41695|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
27530|Owen Conglomerate|41756|6|Mentioned|p189|||||||||
27530|Owen Conglomerate|41795|6|Mentioned|p45|||||||||
27530|Owen Conglomerate|41896|5|Briefly described|p23|||Reference to Newer Volcanics probably intended.||||||04-OCT-07
27530|Owen Conglomerate|41934|6|Mentioned|Map legend|Ordovician||||||||
27530|Owen Conglomerate|42170|4|Described|p136|||||||||
27530|Owen Conglomerate|42209|6|Mentioned|Fig.2 P268|||||||||
27530|Owen Conglomerate|42891|6|Mentioned|p299|||Of the Denison Group.||||||17-JAN-07
27530|Owen Conglomerate|42976|5|Briefly described|p267|||||||||
27530|Owen Conglomerate|43054|4|Described|p10|||At top of  Tyndall Group.||||||04-OCT-07
27530|Owen Conglomerate|43128|5|Briefly described|Fig.6,p476||Early Ordovician|||||||
27530|Owen Conglomerate|43131|5|Briefly described|p566|||||||||
27530|Owen Conglomerate|43133|5|Briefly described|p598|||||||||
27530|Owen Conglomerate|43139|5|Briefly described|p721,Fig.1.|||||||||
27530|Owen Conglomerate|43164|4|Described|1|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43191|5|Briefly described|p52|||||||||
27530|Owen Conglomerate|43239|5|Briefly described|Map Legend|Early Ordovician||||||||
27530|Owen Conglomerate|43241|6|Mentioned|Map Legend|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43242|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43243|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
27530|Owen Conglomerate|43244|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43245|5|Briefly described|Map Legend|Early Devonian|Late Cambrian|||||||
27530|Owen Conglomerate|43246|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43248|6|Mentioned|Map Legend|||of ?Late Cambrian - ?Early Ordovician.||||||
27530|Owen Conglomerate|43249|6|Mentioned|Map Legend|||of ?Late Cambrian - ?Early Ordovician age.||||||
27530|Owen Conglomerate|43250|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Wurawina Supergroup. Equivalent to Denison Group.||||||24-MAY-07
27530|Owen Conglomerate|43560|6|Mentioned|p235|Ordovician|Cambrian|||||||
27530|Owen Conglomerate|43636|6|Mentioned|p280|Early Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|43668|6|Mentioned|p9|||||||||
27530|Owen Conglomerate|43777|5|Briefly described|p4|||||||||
27530|Owen Conglomerate|44012|14|Not recorded|p337|||||||||
27530|Owen Conglomerate|61216|5|Briefly described|p15, p61|Late Cambrian|Late Cambrian|Of the Denison Group. Overlies Tyndall Group; overlain by Moina Sandstone. Massive and poorly bedded, with quartz and rounded to sub-rounded quartzite pebbles and cobbles in an argillite matrix.||||||10-FEB-11
27530|Owen Conglomerate|61260|4|Described|p411|Late Cambrian|Late Cambrian|Four informally named members (Lower Cgl, Middle Sst, Middle Cgl, Upper Sst mbrs). Underlies Gordon Gp; overlies Tyndall Gp; in fault contact with Mount Read Volcanics below. Temporal equivalent in West Coast Range (TAS) of Denison Gp (Denison Range).||||||
27530|Owen Conglomerate|61261|5|Briefly described|p427, p429 Fig. 2|Late Cambrian|Late Cambrian|Comprises 4 informally named members: Lower conglomerate, Middle sandstone, Middle conglomerate and Upper sandstone Members.||||||
27530|Owen Conglomerate|61411|6|Mentioned|p4 Fig.1.|Middle Ordovician|Late Cambrian|Syn-(Tyennan)orogenic sediments accumulated in synclinal cores.||||||
27530|Owen Conglomerate|61412|5|Briefly described|p44, p47 Fig.37, p48.|Middle Ordovician|Late Cambrian|Syn-(Tyennan)orogenic sediments accumulated in synclinal cores. Non-conformable on Murchison Granite and apparently conformable on Tyndall Group.||||||16-MAY-17
27530|Owen Conglomerate|63167|6|Mentioned|p27|Ordovician|Late Cambrian|||||||
27530|Owen Conglomerate|63168|5|Briefly described|p75 Fig. 3.10|Late Cambrian|Late Cambrian|In the Queenstown, Tyndall Range area.||||||
27530|Owen Conglomerate|63169|5|Briefly described|p157 Fig. 5.2, p163|||Includes Pioneer beds in upper section. Discordantly transgresses the Central Volcanic Complex and overlies Tyndall Group volcanics in the Red Hill area; rests discordantly on Murchison Granite elsewhere. Geological Province: Dundas Trough.||||||31-OCT-07
27530|Owen Conglomerate|63170|5|Briefly described|p189, p190|||Includes the Newton Creek Sandstone Member. Predominantly siliceous conglomerate and quartz sandstone. Sections informally referred to as "Lower Owen", "Middle Owen" and "Upper Owen" which may also be referred to as Members (p190).||||||07-FEB-11
27530|Owen Conglomerate|63240|6|Mentioned|p4|||||||||
27530|Owen Conglomerate|63592|6|Mentioned|p41|||Host rock for gold mineralisation.||||||
27530|Owen Conglomerate|63675|6|Mentioned|p14|||Highest grade Cu-Au ores in the North Lyell area occur at or near the contact of this unit, which may be locally hematised, and the Central Volcanic Complex.||||||
27530|Owen Conglomerate|64395|5|Briefly described|p170, p171 Fig. 3, p174 Fig. 8|Late Cambrian|Middle Cambrian|||||||07-FEB-11
27530|Owen Conglomerate|66174|14|Not recorded|?|||||||||
27530|Owen Conglomerate|66623|6|Mentioned|p141.|||Correlated by Webby (1978) with the Nuchea Conglomerate of the Koonenberry Belt, NSW.||||||
27530|Owen Conglomerate|67104|5|Briefly described|p634|Late Cambrian|Late Cambrian|Dundas Trough. Correlates with the Bear Gully Gritstone and Wahroonga Breccia in central Victoria.||||Underlain by the Mount Read Volcanics.||
27530|Owen Conglomerate|67655|6|Mentioned|p14|||||||||
27530|Owen Conglomerate|68314|5|Briefly described|p754, p756, p759|Ordovician|Late Cambrian|Tyennan Orogen.||||Unconformably overlies Tyndall Group.|Conglomerate with lesser breccia and sandstone.|
27530|Owen Conglomerate|68822|6|Mentioned|p331|||||||Unconformably underlain by the Mount Read Volcanics. Overlain by the Gordon Limestone.||
27530|Owen Conglomerate|69369|5|Briefly described|p289, p290 Tb.1  |Early Ordovician|Late Cambrian|Tb.1 includes stratigraphic relationships of Corbett & Komyshan (1989) and Waters & Wallace (1992). Owen Conglomerate appears as a constituent of Owen Group.||||Unconformably overlies Southwell Subgroup.|Pink siliciclastic conglomerate and sandstone.|09-MAY-16
27530|Owen Conglomerate|69773|6|Mentioned|p32|||Ferruginous conglomerate boulders, probably of this unit, occur locally within the Stockers Tillite.||||||
27530|Owen Conglomerate|69851|5|Briefly described|Map legend|||Mentioned as a correlate of a dominantly siliceous conglomerate which is also stated to be a correlate of Mount Zeehan Conglomerate.||||||
27530|Owen Conglomerate|69872|6|Mentioned|p28 Fig.2.11|Ordovician|Ordovician|||||Overlies Tyndall Group. Is overlain by Gordon Limestone.||
27530|Owen Conglomerate|69874|5|Briefly described|p188, p213|||Wade and Solomon (1958). Formerly the West Coast Range Conglomerate (Nye et al., 1934); later the Owen Group (Corbett, 1990). Hellyer-Mount Charter region.||Owen Group||||
27530|Owen Conglomerate|69876|5|Briefly described|p287, 289|Ordovician|Cambrian|Parent group implied. Devonian deformation event described.||Owen Group|||Conglomerate with intense alteration and strong variation in thickness.|
27530|Owen Conglomerate|69880|6|Mentioned|p541|||Auriferous fault-related veins were one source of West Coast alluvial gold.||||||
27530|Owen Conglomerate|70025|4|Described|p2,4,10,13,p18, 26,29|Late Ordovician|Late Cambrian|Burnie Zone, Pedder Zone. Abbreviated as OC on p4 Fig 2.  Locally derived and deposited in half-graben on the west coast of Tasmania and in the north as far east as the eastern part of the Sorell-Badger Head Zone (Noll & Hall 2005; Reed & Vicary 2005), during the waning stage of the Tyennan Orogeny.||||Underlain by Mount Read Volcanics.|Conglomerate, sandstone.|16-JUL-19
27530|Owen Conglomerate|70274|5|Briefly described|p447-448,451|Early Ordovician|Late Cambrian|Also referred to as Oewn Group on p448.||||Underlain conformably to unconformably by Tyndall Group.|Siliciclastic rocks, including shallow marine to fluvial conglomerate and sandstone.|
27530|Owen Conglomerate|70493|6|Mentioned|p56|Late Cambrian|Middle Cambrian|Western Tasmania.||||Overlies Mount Read Volcanics. Is overlain by Wurawina Supergroup.||
27530|Owen Conglomerate|73059|5|Briefly described|p1059|Late Cambrian|Late Cambrian|Western Tasmania.||||Overlies Mount Read Volcanics. Is overlain by Wurawina Supergroup.||
27530|Owen Conglomerate|73170|6|Mentioned|p787, 799|||Now the Owen Group (see references p787-789, 794, 797-798, 801-802, 805-806).||||||
27530|Owen Conglomerate|73430|5|Briefly described|p518|Early Ordovician|Late Cambrian|Latest Cambrian to Earliest Ordovician age. Post-Delamerian.||Dennison Supergroup|||Molassic conglomerate.|
30393|Owen Conglomerate (Group)|43131|6|Mentioned|Fig.9 p582||Late Cambrian|||||||
30393|Owen Conglomerate (Group)|64395|5|Briefly described|p174 Fig. 8.|Late Cambrian|Middle Cambrian|Informal name for units of Owen Conglomerate and associated units.||||||07-FEB-11
28898|Owen Conglomerate beds|33218|6|Mentioned|p41|||||||||
40516|Owen Conglomerate beds, Middle|23948|5|Briefly described|p1099|Late Cambrian|Late Cambrian|||||||
14701|Owen Conglomerate formation|35844|6|Mentioned|p8|||Informal.||||||04-FEB-08
40517|Owen Conglomerate""|23948|5|Briefly described|p1090, p1094 Fig.3|Late Cambrian|Late Cambrian|Also known as the Owen Group - probably upgraded in status?||||||04-FEB-08
40517|Owen Conglomerate""|63170|5|Briefly described|p189|||Informal - see Owen Conglomerate. Three repeated fining-up sequences - each with a basal pebble conglom.followed by sandstone, with a fine-grained conglomerate overlying the top-basal conglomerate. Thickness: 930m+410m+370m.||||||07-FEB-11
40518|Owen Conglomerate, Lower|23948|4|Described|p1090, p1094 Fig.3|Late Cambrian|Late Cambrian|Maximum Thickness: 1200m. Of the Owen Group. Overlies the Zig Zag Hill Formation. Overlain by the Owen Sandstone, MIddle.||||||
40518|Owen Conglomerate, Lower|63238|5|Briefly described|p14, p20 Fig. 3|Late Cambrian|Late Cambrian|Informal division of Owen Group. In Mount Lyell area.||||||
40518|Owen Conglomerate, Lower|63612|6|Mentioned|p11|||In the Mt Lyell area.||||||07-FEB-11
40518|Owen Conglomerate, Lower|63675|6|Mentioned|p13 Fig.8|||Pebble to boulder conglomerate, mostly marine.||||||
40518|Owen Conglomerate, Lower|64395|5|Briefly described|p169, p174 Fig. 8|Late Cambrian|Middle Cambrian|Written as Lower Owen Conglomerate - see Owen Conglomerate.||||||07-FEB-11
40518|Owen Conglomerate, Lower|67655|6|Mentioned|p13 Fig. 8||||||||pebble to boulder conglomerate, mostly non-marine|
40518|Owen Conglomerate, Lower|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Unclear from the legend as to whether this unit is a Formation in Denison or Owen Group.||Unit in Wurawina Supergroup.|||Local lower conglomerate sequences, typically pebble to boulder grade, with sandstone interbeds.|
40518|Owen Conglomerate, Lower|69874|3|Fully described|p149, p202-203, p205-206, p213-214|Idamean|Mindyallan|See also p216-224, p226-227, p233, p240. Queenstown-Henty area. Type section is at the eastern end of Mount Lyell; alternative but mostly faulted sections on Mount Owen. Up to 1500m thick at the Great Lyell Fault, thinning to zero 5km to the E. Lithology described in detail with interpretations. Alluvial fan or slope facies. Uplifted by the North Lyell Fault to form the ridge of Mount Lyell. Poorly fossiliferous.||Owen Group||Overlies Tyndall Group unconformably. Underlies Middle Owen Sandstone.|Pale grey weathering to white, brown or pale pink, thick-bedded to massive, pebble to boulder grade conglomerate with lenses of sandstone and pebbly sandstone. Local basal volcaniclastic conglomerate or a siltstone-sandstone unit.|
40518|Owen Conglomerate, Lower|70753|5|Briefly described|p184-185|||Up to 1500m thick.||Owen Group.||Unconformably overlies Tyndall Group. Is overlain by Middle Owen Sandstone.|Coarse conglomerate.|
40518|Owen Conglomerate, Lower|71706|5|Briefly described|p209,217|Late Cambrian|Late Cambrian|Informal. Deposited by fluvial, alluvial fan processes. Also  called 'Lower Conglomerate Member' in Table 1 p212.||Of Owen Group.||Oldest unit of the Owen Group. Locally overlies Jukes Conglomerate.|Boulder cobble conglomerate and coarse grained sandstone.|
40518|Owen Conglomerate, Lower|73320|5|Briefly described|Map legend|Furongian|Furongian|Western Tasmania. Overlies angular unconformity in some areas, apparent conformity in others. Grouped in either Owen Group, Dension Group and correlates.|||||Included in lower conglomerate sequences in some areas, typically pebble to boulder grade, with sandstone interbeds.|
40518|Owen Conglomerate, Lower|73489|5|Briefly described|p653, p655|Furongian|Furongian|Western Tasmania. See also lower Owen conglomerate p660.||||Overlies Mount Read Volcanics, underlies Middle Owen Conglomerate and correlates|Conglomerate.|
40518|Owen Conglomerate, Lower|75070|5|Briefly described|p178|Furongian|Furongian|Western Tasmania.||||Unconformably overlies Mount Read Volcanics. Is overlain by Middle Owen Conglomerate.|Conglomerate.|
40519|Owen Conglomerate, Middle|23948|4|Described|p1090, p1094 Fig.3|Late Cambrian|Late Cambrian|Maximum Thickness: 150m. Of the Owen Group. Overlies the Middle Owen Sandstone. Overlain by the Upper Owen Sandstone.||||||
40519|Owen Conglomerate, Middle|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Late Cambrian|Informal division of Owen Group.||||||
40519|Owen Conglomerate, Middle|63612|6|Mentioned|p11|||In the Mt Lyell area.||||||07-FEB-11
40519|Owen Conglomerate, Middle|64395|5|Briefly described|p174 Fig. 8.|Late Cambrian|Late Cambrian|Informal name for middle section of Owen Conglomerate.||||||07-FEB-11
40519|Owen Conglomerate, Middle|69857|5|Briefly described|Map legend|Ordovician|Cambrian|||Unit in Owen Group.|||Mainly siliciclastic pebble to boulder conglomerate with sandstone interbeds, shallow-marine to non-marine.|
40519|Owen Conglomerate, Middle|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Unclear from the legend as to whether this unit is a Formation in Denison or Owen Group.||Unit in Wurawina Supergroup.|||Mainly quartz-rich pebble to boulder conglomerate with sandstone interbeds; shallow-marine to non-marine.|
40519|Owen Conglomerate, Middle|69874|4|Described|p202-203, p206, p213-214, p216-217, p219|||See also p221-224, p227, p230-231, p233. West Coast Range area. 40-350m thick; wedges out to the E. Essentially identical to Lower Owen Conglomerate; mostly fluvial and represents a similar alluvial fan or slope facies. Lithology detailed. Includes numerous clasts of a distinctive hematite-jasper-barite vein material in a so-called "jasper bed".||Owen Group||Overlies Newton Creek / Middle Owen Sandstone. Is overlain by and interfingers with Upper Owen Sandstone.|Pink to pale pink-grey, thick-bedded to massive, pebble-cobble to cobble-boulder conglomerate with sandstone lenses. Contains breccias and conglomerates rich in red-purple hematite and/or white chert.|
40519|Owen Conglomerate, Middle|70753|5|Briefly described|p185|||40-350m thick.||Owen Group.||Overlies Lower Owen Conglomerate. Is overlain by Middle Owen Conglomerate. Equivalent to Newton Creek Formation.|Coarse conglomerate.|
40519|Owen Conglomerate, Middle|71706|4|Described|p209,p212 Table 1, 217|Late Cambrian|Late Cambrian|Informal.||Of Owen Group.||Overlies Middle Owen Sandstone.|Boulder-cobble conglomerate and coarse fluvial sandstone.|
40519|Owen Conglomerate, Middle|73313|6|Mentioned|Map legend|Furongian|Furongian|Map unit includes Middle Owen Conglomerate, Dial Conglomerate, Roland Conglomerate; description of mainly siliciclastic conglomerate with sandstone interbeds, shallow marine to non-marine, pebble to boulder grade.||Owen Group||||
40519|Owen Conglomerate, Middle|73320|6|Mentioned|Map legend|Furongian|Furongian|Western Tasmania. Map unit includes Middle Owen Conglomerate, Mount Zeehan Conglomerate, Roland Conglomerate; description of mainly quartz-rich conglomerate with sandstone interbeds, shallow marine to non-marine, pebble to boulder grade. Grouped in either Owen Group, Dension Group and correlates.||||||
40519|Owen Conglomerate, Middle|73489|5|Briefly described|p653|Furongian|Furongian|Western Tasmania.||||Overlies Lower Owen Conglomerate, underlies Upper Owen Sandstone|Sandstone, conglomerate.|
40519|Owen Conglomerate, Middle|75070|5|Briefly described|p178|Furongian|Furongian|Western Tasmania.||||Overlies Lower Owen Conglomerate. Is overlain by Upper Owen Sandstone.|Conglomerate, sandstone.|
73815|Owen Conglomerate, upper|63169|6|Mentioned|p163|||Informal - see Owen Conglomerate.||||||
26826|Owen Formation|638|5|Briefly described|p104|||Transgresses unconformably across the Tyndall Group at South Darwin Peak and rests directly on the Central Volcanic Complex in the range. Unclear how Owen Formation relates to Owen Conglomerate?||||||
26826|Owen Formation|30275|6|Mentioned|p118|||||||||
26826|Owen Formation|30276|5|Briefly described|p19|||||||||
26826|Owen Formation|30278|6|Mentioned|p174|||Unconformity in upper part of Fm. Refs Wade and Solomon 1958.||||||04-FEB-08
26826|Owen Formation|30281|6|Mentioned|p16|||||||||
26826|Owen Formation|32627|6|Mentioned|p22|Ordovician|Ordovician|Flaggy, white, shallowly-dipping quartzite beds.||||||07-FEB-08
26826|Owen Formation|35844|6|Mentioned|p10|||Fossil content.||||||
26826|Owen Formation|37046|6|Mentioned|p237|||||||||
26826|Owen Formation|37047|6|Mentioned|p247|||||||||
26826|Owen Formation|40070|6|Mentioned|p12|||||||||
26826|Owen Formation|40662|6|Mentioned|p181|||||||||
26826|Owen Formation|41795|6|Mentioned|Fig.3|Ordovician||||||||
40520|Owen Formation, Lower|23948|6|Mentioned|p1110|||Informal - see the Owen Group.||||||
78336|Owen Formation, Middle|63675|6|Mentioned|p13 Fig.8|||Sandstone and pebble conglomerate, mostly marine.||||||
78336|Owen Formation, Middle|67655|6|Mentioned|p13 Fig. 8||||||||sandstone and pebble conglomerate, mostly marine|
78336|Owen Formation, Middle|69874|6|Mentioned|p201, p205|||Associated with the Iron Blow Cu sulfide orebody.||Owen Group||||
78337|Owen Formation, Upper|63675|6|Mentioned|p13 Fig.8|||Sandstone and pebble conglomerate, mostly marine.||||||
78337|Owen Formation, Upper|67655|6|Mentioned|p13 Fig. 8||||||||sandstone and pebble conglomerate, mostly marine|
78337|Owen Formation, Upper|69874|6|Mentioned|p201, p205|||||Owen Group||||
73116|Owen Group, Lower|44135|5|Briefly described|p18, p19||Late Cambrian|Informal - see Owen Group. Thick bedded and massive conglomerate part of sequence, up to boulder grade; and a thin unit of siltstone and sandstone.||||||07-DEC-09
73116|Owen Group, Lower|73489|6|Mentioned|p654 Tb.1, p655|||Western Tasmania. See also lower Owen Group p655.|||||Includes sandstone.|
73117|Owen Group, Middle|44135|5|Briefly described|p18, p19|||Informal - see Owen Group. Thick bedded and massive conglomerate part of sequence, pebble-cobble and cobble-pebble conglomerate with thin lenses of pink sandstone.||||||07-DEC-09
73117|Owen Group, Middle|73489|6|Mentioned|p654 Tb.1|||Western Tasmania.|||||Includes sandstone.|
83502|Owen Group, Upper|73489|6|Mentioned|p654 Tb.1|||Western Tasmania.|||||Includes sandstone, conglomerate.|
83505|Owen Group, lower|73489|6|Mentioned|p655, p656|||See also Lower Owen Group.|||||Sedimentary rocks.|07-SEP-22
83498|Owen Group, upper|73489|6|Mentioned|p651, p656 Fig.3, p662|||See also Upper Owen Group p654 Tb.1.||||||
40521|Owen Sandstone, Middle|23948|4|Described|p1090, p1094 Fig.3|Late Cambrian|Late Cambrian|Maximum Thickness: 150m. Of the Owen Group. Overlies the Lower Owen Conglomerate. Overlain by the Middle Owen Conglomerate.||||||
40521|Owen Sandstone, Middle|69857|5|Briefly described|Map legend|Ordovician|Cambrian|||Unit in Owen Group.|||Part of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, siliciclastic to polymict.|
40521|Owen Sandstone, Middle|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Unclear from the legend as to whether this unit is a Formation in Denison or Owen Group.||Unit in Wurawina Supergroup.|||Marine sandstone-siltstone-conglomerate sequences, typically turbiditic, quartz-rich to polymict; Furongian fossils in places.|
40521|Owen Sandstone, Middle|69874|3|Fully described|p202-203, p206, p213, p216-217, p219|||See also p221-224, p227. Mount Lyell (West Coast Range) area. 140-1000m thick. Type area is at the eastern end of Mount Lyell, where it is 150m thick. Lithology detailed.||Owen Group.||Overlies the Lower Owen Conglomerate.|Pink to reddish-brown, hematitic, cross-bedded sandstone, changing facies to the N into a grey marine sandstone-siltstone sequence called the Newton Creek Sandstone. Contains breccias and conglomerates rich in red-purple hematite and/or white chert.|
40521|Owen Sandstone, Middle|70753|5|Briefly described|p185|||140-1000m thick.||Owen Group.||Overlies Middle Owen Sandstone. Is overlain by Upper Owen Sandstone.||
40521|Owen Sandstone, Middle|71706|4|Described|p209,217|Late Cambrian|Late Cambrian|Informal. Proximal marine turbidite facies north of Mount Julia. Also  called 'Middle Sandstone Member' in Table 1 p212, and Newton Creek Sandstone north of Mount Julia. ||Of Owen Group.||Overlies Lower Owen Conglomerate. Equivalent to Newton Creek Sandstone?|High energy fluvial sandstone south of the Tyndall Range and proximal marine turbidite facies north of Mount Julia. |
40521|Owen Sandstone, Middle|73313|6|Mentioned|Map legend|Furongian|Furongian|Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, siliciclastic to polymict, Furongian fossils in places.||Owen Group||||
40521|Owen Sandstone, Middle|73320|6|Mentioned|Map legend|Furongian|Furongian|Western Tasmania. Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, quartz-rich to polymict; Furongian fossils in places. Grouped in either Owen Group, Dension Group and correlates.||||||
40523|Owen Sandstone, Upper|23948|4|Described|p1090, p1094 Fig.3|Late Cambrian|Late Cambrian|Maximum Thickness: 150. Of the Owen Group. Overlies the Upper Owen Sandstone [???can't overlie itself]. Unconformably overlain by the Pioneer Sandstone.||||||03-FEB-11
40523|Owen Sandstone, Upper|24601|6|Mentioned|p847|||Informal variation on 'upper sandstone member' of the Owen Conglomerate?  In contact with the Pioneer Sandstone.||||||30-NOV-09
40523|Owen Sandstone, Upper|44135|5|Briefly described|p18, p19, p27|Early Ordovician||Informal - see Owen Group. Shallow marine sequence( including Pioneer Beds?); chert-rich granule-pebble conglomerate.||||||07-DEC-09
40523|Owen Sandstone, Upper|63238|5|Briefly described|p11, p20 Fig. 3|Late Cambrian|Late Cambrian|Informal division of Owen Group. Comprises a thick sandstone sequence with mudcrack infills preserved in places. ||||||
40523|Owen Sandstone, Upper|69857|5|Briefly described|Map legend|Ordovician|Cambrian|||Unit in Owen Group.|||Shallow marine sandstone, typically pink, cross-bedded to thin-bedded with some siltstone and minor conglomerate.|
40523|Owen Sandstone, Upper|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Unclear from the legend as to whether this unit is a Formation in Denison or Owen Group.||Unit in Wurawina Supergroup.|||Shallow-marine sandstone, typically pink, cross-bedded to thin-bedded, with some siltstone and minor conglomerate.|
40523|Owen Sandstone, Upper|69874|4|Described|p201-203, p206-207, p213-214, p216-217|Early Ordovician|Early Ordovician|See also p219, p221-230. West Coast Range area. Shallow-marine to deltaic and fluvial sequence. 200-500m thick. Lithology detailed. Beds are locally upturned, overturned and folded: the Haulage Fold Zone. No age-diagnostic fossils; upper age is uncertain. Sparse to abundant trace fossils. Age from stratigraphic correlation.||Owen Group||Gradationally overlies Middle Owen Conglomerate. Is overlain by Pioneer Sandstone disconformably to unconformably, or Gordon Group conformably.|Pink to grey interbedded sandstone, siltstone and granule-pebble conglomerate. Contains breccias and conglomerates rich in red-purple hematite and/or white chert.|
40523|Owen Sandstone, Upper|69875|5|Briefly described|p243 Fig 5.2, p246-247|Early Ordovician|Cambrian|Queenstown, Moina district. Age is poorly constrained.||Owen Group||Unconformably underlies Cattley Sandstone, Pioneer Sandstone, Moina Sandstone.|Sandstone.|
40523|Owen Sandstone, Upper|70753|5|Briefly described|p185|||200-500m thick.||Owen Group.||Overlies Middle Owen Conglomerate.||
40523|Owen Sandstone, Upper|71706|4|Described|p209, p212 Table 1, 217|Late Cambrian|Late Cambrian|Informal.||Of Owen Group.||Overlies Middle Owen Conglomerate; unconformably overlies basement in places.|Variously cross bedded, gritty medium-grained sandstone, pebbly conglomerate and thin shale beds.|
40523|Owen Sandstone, Upper|73313|5|Briefly described|Map legend|Ordovician|Furongian|||Owen Group|||Included in shallow marine sandstone, typically pink, cross-bedded to thin-bedded with some siltstone and minor conglomerate.|
40523|Owen Sandstone, Upper|73320|5|Briefly described|Map legend|Furongian|Furongian|Western Tasmania. Grouped in either Owen Group, Dension Group and correlates.|||||Included in shallow marine sandstone, typically pink, cross-bedded to thin-bedded, with some siltstone and minor conglomerate.|
40523|Owen Sandstone, Upper|73489|5|Briefly described|p653||Early Ordovician|Underlies Haulage Unconformity.||||Overlies Middle Owen Conglomerate and correlates, unconformably underlies Pioneer Sandstone, Gordon Group|Sandstone.|
40523|Owen Sandstone, Upper|75070|5|Briefly described|p178, 180-181|Early Ordovician|Early Ordovician|Western Tasmania. Detrital zircon graph. Hf isotope diagram.||||Overlies Middle Owen Conglomerate. Is overlain unconformably by Pioneer Sandstone and Gordon Group.|Sandstone.|
74935|Owen Sandstones, Upper|64395|5|Briefly described|p174 Fig. 8|Ordovician|Late Cambrian|Informal name - probably refers to the top bed of the Owen Conglomerate which is shown to have Middle and Lower sections in Figure 8.||||||07-FEB-11
14708|Owen beds|23948|6|Mentioned|p1110|||||||||
14708|Owen beds|30281|6|Mentioned|p9|||||||||
14708|Owen beds|40070|6|Mentioned|p17|||||||||
14708|Owen beds|43164|6|Mentioned|23||Cambrian|||||||
14708|Owen beds|63238|6|Mentioned|p16|||Informal reference to sections of the Owen Group. ||||||
40514|Owen beds, Upper|23948|6|Mentioned|p1098|||Informal - see Owen beds.||||||
40515|Owen conglomerate|23948|6|Mentioned|p1089|||Informal - see Owen Conglomerate||||||
40528|Owen conglomerate, Lower|23948|6|Mentioned|p1110|||Informal - see Owen Conglomerate||||||
34171|Owen conglomerate, Middle""|22627|6|Mentioned|p132|Cambrian|Cambrian|||||||
83506|Owen conglomerate, lower|73489|6|Mentioned|p660|||See also Lower Owen Conglomerate.||||||
14709|Owen conglomerates|33281|6|Mentioned|p11|||Mt. Lyell orebody country rock.||||||
14710|Owen formation|40736|6|Mentioned|Fig.1|||||||||
14710|Owen formation|41148|6|Mentioned|Fig.2|||||||||
40522|Owen sandstone, Middle|23948|6|Mentioned|p1110|||Informal - see Owen Group||||||
83504|Owen sandstone, middle|73489|6|Mentioned|p655|||||||||
73818|Owen sandstone, upper|63169|6|Mentioned|p166 Fig. 7.7|||Informal reference to sandstone within the Owen sequence - probably refers to the upper Owen Conglomerate? ||||||
73818|Owen sandstone, upper|73489|6|Mentioned|p655|||See also Upper Owen Sandstone p653.||||||
14711|Owen"" conglomerates|33738|6|Mentioned|p46|||||||||
14715|Owens Conglomerate|45130|6|Mentioned|p15|||Misspelling of Owen?||||||
14718|Own Conglomerate|33218|6|Mentioned|p11|||Misspelling of Owen?||||||
14803|Palmer Formation|24549|4|Described|p6|Permian|Permian|Of the Ferntree Group. Max. Thickness: 5ft. Poorly sorted quartz feldspar sandstone containing pebbles of slate, mica schist and quartzite||||||27-SEP-07
14803|Palmer Formation|30156|6|Mentioned|p40|||Part of Bogan Gap Group||||||
14803|Palmer Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Upper Permian. Part of the Ferntree Group. Quartz feldspar sandstone.||||||06-FEB-08
14803|Palmer Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Permian|Early Permian|Informally named in chart Fig. 8.1 - and should be Palmer Sandstone. Of the Bogan Gap Group.||||||07-FEB-11
14803|Palmer Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
14803|Palmer Formation|63890|5|Briefly described|p15|Late Permian|Late Permian|Mentioned in terms of correlate rocks.||||||
14806|Palmer Sandstone""|30889|6|Mentioned|p50|||||||||
39918|Palmer sandstone|24549|6|Mentioned|Map 4885|||||||||27-SEP-07
39316|Parameener Supergroup|24408|6|Mentioned|p35|Late Triassic|Late Carboniferous|Geological Province: Tasmania Basin||||||03-MAR-05
14863|Parameener Supergroup Lower|24408|6|Mentioned|p35|||Geological Province: Tasmania Basin||||||03-MAR-05
14863|Parameener Supergroup Lower|42227|4|Described|p53-54|Late Permian|Late Carboniferous|An accepted stratigraphic nomenclatural term but should be an informal term. Part of the Parmeener Supergroup. Includes descriptions of unnamed conglomerate, pebbly mudstone, fossiliferous pebbly mudstone, sandstone and fossiliferous sandstone/siltstone/m||||||16-JUN-09
39317|Parameener Supergroup, Upper|24408|6|Mentioned|p35|Norian|Permian|Geological Province: Tasmania Basin||||||03-MAR-05
83429|Parmeener Group|71540|6|Mentioned|p292|||Density values used to calculate volume of deposited sediment after flooding.||||||
83430|Parmeener Group, Lower|71540|6|Mentioned|p293 Fig.4|||||||||
18941|Parmeener Group, Upper|39579|6|Mentioned|p19|||||||||
18941|Parmeener Group, Upper|71540|6|Mentioned|p293 Fig.4|||||||||
14891|Parmeener Subgroup|41793|4|Described|p58|||Misspelling of Parmeener Supergroup? Comment added 1993.||||||
14891|Parmeener Subgroup|42348|5|Briefly described|p1|Triassic|Permian|||||||
14891|Parmeener Subgroup|43584|5|Briefly described|p57|Triassic|Permian|||||||
74068|Parmeener Subgroup, upper|63604|5|Briefly described|p966|Late Triassic|Permian|Consists of terrestrial siliciclastic and volcaniclastic beds and contains intrusives dated at 233+/-5Ma. See also p966.||||||
14892|Parmeener Super Group|30280|6|Mentioned|Map legend|Permian|Late Carboniferous|Upper Carboniferous - Triassic||||||
14892|Parmeener Super Group|30521|6|Mentioned|Map legend|Permian|Late Carboniferous|Upper Carboniferous - Triassic||||||
14892|Parmeener Super Group|30927|6|Mentioned|Map legend|Permian|Late Carboniferous|Triassic to Upper Carboniferous||||||
14892|Parmeener Super Group|31766|6|Mentioned|p61|||||||||
14892|Parmeener Super Group|32093|6|Mentioned|Map legend|Triassic|Carboniferous|Carboniferous to Triassic||||||
14892|Parmeener Super Group|35153|6|Mentioned|p201|||||||||
14892|Parmeener Super Group|35203|6|Mentioned|Map legend|Permian|Late Carboniferous|||||||
14892|Parmeener Super Group|35828|6|Mentioned|Map legend|Permian|Late Carboniferous|||||||
18942|Parmeener Super Group, Upper|37009|6|Mentioned|p177|||||||||
14896|Parmeener Super-Group|29609|6|Mentioned|Fig.1|||||||||
14896|Parmeener Super-Group|30150|6|Mentioned|p93|||||||||
14896|Parmeener Super-Group|30155|4|Described|p455|||Biostratigraphy||||||
14896|Parmeener Super-Group|30281|4|Described|p12|||||||||
14896|Parmeener Super-Group|30718|6|Mentioned|Map legend|Late Triassic|Late Carboniferous|Upper Carboniferous - Triassic||||||
14896|Parmeener Super-Group|30819|4|Described|p107|||Late Carboniferous - Late Triassic age.||||||
14896|Parmeener Super-Group|32094|6|Mentioned|p382|||||||||
14896|Parmeener Super-Group|33840|6|Mentioned|Map legend|Triassic|Carboniferous|Carb. - Triassic||||||
14896|Parmeener Super-Group|35818|4|Described|p7|||||||||
14896|Parmeener Super-Group|35819|4|Described|p10|||||||||
14896|Parmeener Super-Group|36350|6|Mentioned|p6|||||||||
14896|Parmeener Super-Group|36682|5|Briefly described|Fig.1|||||||||
14896|Parmeener Super-Group|36787|6|Mentioned|Map legend|Triassic|Permian|Triassic to Permian.||||||
14896|Parmeener Super-Group|36941|6|Mentioned|p163|||||||||
14896|Parmeener Super-Group|37102|6|Mentioned|p264|||||||||
14896|Parmeener Super-Group|37108|6|Mentioned|p282|||||||||
14896|Parmeener Super-Group|37135|5|Briefly described|p300|||||||||
14896|Parmeener Super-Group|38200|6|Mentioned|p67|||||||||
14896|Parmeener Super-Group|39235|6|Mentioned|Map legend|Triassic|Carboniferous|Carboniferous to Triassic||||||
14896|Parmeener Super-Group|39579|3|Fully described|p9|||||||||
14896|Parmeener Super-Group|39777|6|Mentioned|p137|||||||||
14896|Parmeener Super-Group|39916|6|Mentioned|Map legend|Permian|Permian|||||||
14896|Parmeener Super-Group|40760|6|Mentioned|p190|||||||||
14896|Parmeener Super-Group|41793|6|Mentioned|p45|||||||||
14896|Parmeener Super-Group|41818|4|Described|p7|||||||||
14896|Parmeener Super-Group|41895|5|Briefly described|p9|||Described in two parts: Lower Division P9 and Upper Division P48||||||
14896|Parmeener Super-Group|41896|4|Described|p31|||||||||
14896|Parmeener Super-Group|42185|6|Mentioned|p365|||||||||
14896|Parmeener Super-Group|42648|5|Briefly described|p49|||Misspelling of Parmeener Supergroup||||||
14896|Parmeener Super-Group|43072|5|Briefly described|p37|||||||||
14896|Parmeener Super-Group|43078|5|Briefly described|p15|||||||||
14896|Parmeener Super-Group|46849|6|Mentioned|p197|||||||||
14896|Parmeener Super-Group|69852|5|Briefly described|Map legend|Triassic|Permian|||||Unconformably overlies Mathinna Beds.|Conglomerate and sandstone.|
14895|Parmeener Super-Group siliclastics|36941|6|Mentioned|p163|||||||||
14893|Parmeener Super-Group, Lower|41818|6|Mentioned|p7|||||||||
14893|Parmeener Super-Group, Lower|41855|3|Fully described|p14|||Also Desc p13.||||||27-MAR-19
14893|Parmeener Super-Group, Lower|41895|5|Briefly described|p9|||||||||
14893|Parmeener Super-Group, Lower|43078|6|Mentioned|p89|||||||||
14894|Parmeener Super-Group, Upper|41855|3|Fully described|p30|||||||||
14894|Parmeener Super-Group, Upper|41895|4|Described|p48|||||||||
14894|Parmeener Super-Group, Upper|43078|6|Mentioned|p89|||||||||
14897|Parmeener Super-group|35671|6|Mentioned|Fig.1|||Geological sketch map.||||||
14897|Parmeener Super-group|37926|4|Described|p495|||||||||
14897|Parmeener Super-group|40706|6|Mentioned|p23|||||||||
14897|Parmeener Super-group|61395|6|Mentioned|p7|||Informal - see Parmeener Supergroup.||||||07-FEB-11
14901|Parmenteer Supergroup|35647|6|Mentioned|?|||Misspelling of Parmeener Supergroup. [CEBMar95]||||||
73630|Patriarchs Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Wybalenna Suite. I-type, felsic granite; moderately to strongly fractionated, reduced. Name implied from map legend.||||||25-SEP-07
73630|Patriarchs Granite|69876|5|Briefly described|p306 Tb 6.1|Devonian|Devonian|Age inferred.||Poimena Suite|||I-type biotite adamellite-granite.|
73630|Patriarchs Granite|71730|6|Mentioned|p33, p35, p37, p57||||||||I type granite.|
81979|Pats River Granodiorite|71730|6|Mentioned|p26,32,33, p35, p37, p43, p49,51, p57|Devonian|Devonian|Flinders Island. Low heat generation. Granodiorite name implied only on p43. Granite implied on other pages.|||||Unfractionated I-type granodiorite.|09-NOV-20
14979|Pearson granite|37797|6|Mentioned|p139|||Variation of Mount Pearson?||||||
79593|Pebble Beds Member|69876|5|Briefly described|p342-343|Ordovician|Ordovician|Beaconsfield Gold Mine informal stratigraphy. Name from unpublished sources.Previously assigned to underlying Salisbury Hill Formation (Lewis, 1998). Reassigned by Hills et al. (2004).||Eaglehawk Gully Formation||Overlies Salisbury Hill Formation conformably.|Calcareous quartz sandstone with minor pebble layers and very minor limestone.|16-JAN-17
15030|Pember Mudstone|12781|6|Mentioned|p386|Eocene|Paleocene|Otway Basin. Maximum thickness 196m.||Wangerip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation, locally unconformably.||
15030|Pember Mudstone|12796|5|Briefly described|p456 Fig. 2|Thanetian|Thanetian|Geological Province: Otway Basin.||||||
15030|Pember Mudstone|22674|5|Briefly described|Fig.2 p719|Early Eocene|Early Paleocene|||||||
15030|Pember Mudstone|22875|3|Fully described|p52|Early Eocene|Late Paleocene|Of the Wangerrip Group.||||||30-JAN-07
15030|Pember Mudstone|22944|5|Briefly described|Fig3|Eocene|Paleocene|||||||
15030|Pember Mudstone|23307|5|Briefly described|Map Legend|Paleocene|Paleocene|Of Wangerrip Group.||||||24-JUL-08
15030|Pember Mudstone|23322|5|Briefly described|957 Fig.2|Eocene|Paleocene|Of the Wangerrip Group.  Geological Province: Gambier Basin.||||||07-SEP-09
15030|Pember Mudstone|23778|5|Briefly described|p668|||Of Eastern View Group. Otway Basin.||||||
15030|Pember Mudstone|24038|5|Briefly described|p439 Fig.2|Paleocene|Paleocene|Geological Province: Torquay Basin.||||||24-JUL-08
15030|Pember Mudstone|24202|5|Briefly described|p313 Fig. 2|Late Paleocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Sub-basin.||||||06-FEB-08
15030|Pember Mudstone|24314|5|Briefly described|p61 Fig.2||Late Paleocene|Geological Province: Otway Basin. Max. Thickness 198m. Of the Wangerrip Group.||||||30-NOV-04
15030|Pember Mudstone|24551|5|Briefly described|p246, 295|Eocene|Paleocene|Of the Wangerrip Group.||||||13-DEC-21
15030|Pember Mudstone|24562|5|Briefly described|p8 Fig. 2|Eocene|Paleocene|Of the Wangerrip Group.  Geological Province: Otway Basin.||||||
15030|Pember Mudstone|30578|5|Briefly described|p8|||||||||
15030|Pember Mudstone|31372|6|Mentioned|Fig. 2|||||||||
15030|Pember Mudstone|31424|6|Mentioned|Plate 1|||Shown in composite bore log.||||||
15030|Pember Mudstone|31625|6|Mentioned|Fig. 5.2|||Palaeocene||||||
15030|Pember Mudstone|36366|6|Mentioned|p9|||||||||
15030|Pember Mudstone|36913|6|Mentioned|p81|||||||||
15030|Pember Mudstone|37548|6|Mentioned|p131|||||||||
15030|Pember Mudstone|41016|5|Briefly described|Table 1|||||||||
15030|Pember Mudstone|41185|6|Mentioned|p178|||See also Fig.4||||||
15030|Pember Mudstone|41269|5|Briefly described|p246|||||||||
15030|Pember Mudstone|41704|6|Mentioned|Fig.3|||||||||
15030|Pember Mudstone|41714|6|Mentioned|Fig.2|||||||||
15030|Pember Mudstone|41726|6|Mentioned|p428|||||||||
15030|Pember Mudstone|41868|4|Described|p534|||||||||
15030|Pember Mudstone|42079|6|Mentioned|Fig.2 P264|||||||||
15030|Pember Mudstone|42453|6|Mentioned|p11|||||||||
15030|Pember Mudstone|42524|5|Briefly described|Fig.3 P27|||||||||
15030|Pember Mudstone|42555|5|Briefly described|Fig.2 P285|||||||||
15030|Pember Mudstone|42599|5|Briefly described|Fig.3 P614|||||||||
15030|Pember Mudstone|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
15030|Pember Mudstone|43171|6|Mentioned|5-8|||Of Wangerrip Group. Age: 45-65Ma||||||
15030|Pember Mudstone|43195|5|Briefly described|Map Legend|Eocene|Paleocene|See also commentary on back of map. Of Wangerrip Group||||||
15030|Pember Mudstone|43208|5|Briefly described|map legend|Early Eocene|Late Paleocene|Of Wangerrip Group||||||
15030|Pember Mudstone|43219|5|Briefly described|Fig.3,p6.|Eocene|Maastrichtian|Of the Wangerrip Group.||||||27-SEP-07
15030|Pember Mudstone|43590|4|Described|p18|Early Eocene|Late Paleocene|||||||
15030|Pember Mudstone|43660|6|Mentioned|Fig.6,p15|Eocene|Paleocene|||||||
15030|Pember Mudstone|43733|6|Mentioned|Fig.2.11,p65|Eocene|Paleocene|||||||
15030|Pember Mudstone|43744|6|Mentioned|Fig.3,p3|||||||||
15030|Pember Mudstone|43814|6|Mentioned|Fig.3,p115|||||||||
15030|Pember Mudstone|43937|5|Briefly described|Map Legend|Paleocene|Santonian|||||||
15030|Pember Mudstone|44133|5|Briefly described|p154|Early Eocene|Late Paleocene|Of the Wangerrip Group. Geological Province: Gambier Basin. Interfingers with Dilwyn Formation. ||||||
15030|Pember Mudstone|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
15030|Pember Mudstone|61017|5|Briefly described|p5 Fig. 2|Lutetian|Selandian|Of the Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
15030|Pember Mudstone|61155|5|Briefly described|p18|Middle Eocene|Early Paleocene|Of the Wangerrip (Knight) Group. Overlies Pebble Point Formation; over and under and interfingers with Mussel Formation. Geological Province: Otway Basin (Port Campbell and Tyrendarra  Embayments). ||||||
15030|Pember Mudstone|61182|5|Briefly described|p19, p21-22, p169|Early Eocene|Late Paleocene|Of Wangerrip Gp. Considered by some as part of Dilwyn Formation but here treated as separate formation. Conformable on Pebble Point Fm. and Moomowroong Sand; conformable below Dilwyn Fm. Geol.Prov: Otway Basin. Carbonaceous, micaceous, pyritic; burrowed.||||||07-NOV-08
15030|Pember Mudstone|61470|5|Briefly described|p28 Fig. 5|Lutetian|Selandian|Of the Wangerrip Group. Underlain by and interfingers with Pebble Point Formation; overlain by and interfingers with Dilwyn Formation.  Geological Province: Otway Basin.||||||27-MAY-06
15030|Pember Mudstone|61547|6|Mentioned|p461 Fig.2. |Eocene|Paleocene|||Unit in Wangerrip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation.||
15030|Pember Mudstone|61622|5|Briefly described|p436 Fig. 2|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-FEB-11
15030|Pember Mudstone|61623|6|Mentioned|p449 Fig. 4|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
15030|Pember Mudstone|61626|5|Briefly described|p486, p486 Fig. 2, p488 Fig. 4|Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
15030|Pember Mudstone|61627|5|Briefly described|p500 Fig. 2|Eocene|Paleocene|Of Wangerrip Group. Overlain by Dilwyn Formation, underlain by Pebble Point Formation. Geological Province: Otway Basin.||||||19-SEP-12
15030|Pember Mudstone|61628|5|Briefly described|p509 Fig. 3|Middle Eocene|Paleocene|Of Wangerrip Group. Geological Province: Otway Basin.||||||07-APR-09
15030|Pember Mudstone|62896|5|Briefly described|p88, p89|||Abbreviated version of Pember Mudstone Member found at base of Dilwyn Formation (Wangerrip Group). Thickness: almost 60m. See also Pember Mudstone Member. See also p91.||||||07-FEB-11
15030|Pember Mudstone|63122|5|Briefly described|p17 Fig. 4.3|Early Eocene|Late Paleocene|Of the Wangerrip Group. Max. thickness: 198m. Geological Province: Otway Basin. ||||||
15030|Pember Mudstone|63124|3|Fully described|p49 Fig. 5.2, p87 Fig. 5.29, p88|Early Eocene|Late Paleocene|Of the Wangerrip Group. Synonymous with Burrungule Member of the Tartwaup Formation (Harris 1966). Conformably overlies Pebble Point Formation; overlies Dilwyn Formation. Age: ~59-~49.5Ma. Max. thickness: 200m. Geological Province: Otway Basin.||||||
15030|Pember Mudstone|63129|5|Briefly described|p137|Early Tertiary|Early Tertiary|Geological Province: Otway Basin. May act as a regional seal, and together with Pebble Point Formation is the only seal for the condensed Sherbrook Group. ||||||
15030|Pember Mudstone|63130|5|Briefly described|p143|Tertiary|Tertiary|Geological Province: Otway Basin.||||||06-FEB-08
15030|Pember Mudstone|63269|5|Briefly described|p605|Eocene|Paleocene|Otway Basin.||Wangerrip Group.||||
15030|Pember Mudstone|63431|5|Briefly described|p677 Fig. 2|Eocene|Paleocene|Of the Wangerrip Group. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
15030|Pember Mudstone|63740|6|Mentioned|p88|||Part of the Dilwyn Formation?  See also Pember Mudstone Member - names used interchangeably in study.||||||07-FEB-11
15030|Pember Mudstone|66002|6|Mentioned|p10 Tb.8|||Of Tickell et al. 1992, Edwards et al. 1994, and herein.||||||
15030|Pember Mudstone|66245|5|Briefly described|p6 Fig.5. |Lutetian|Selandian|||Unit in Wangerrip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation.||
15030|Pember Mudstone|67061|5|Briefly described|p545, p546 Fig.3.|Paleocene|Paleocene|Otway Basin. Coal measures and underlying mudstones and sandstones in this unit have sedimentological and stratigraphic affinities with similar facies in onshore Eastern View Group (Torquay Sub-basin). ||Unit in Wangerrip Group.||||
15030|Pember Mudstone|67366|5|Briefly described|p103 Fig.2. |Eocene|Paleocene|||Unit in Wangerrip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation.|Shelf to open marine shale.|
15030|Pember Mudstone|67367|5|Briefly described|p131 Fig.2. |Middle Eocene|Late Paleocene|||Unit in Wangerrip Group.||||
15030|Pember Mudstone|68116|5|Briefly described|Appendix, Map 54.|Eocene|Paleocene||||||Silty clay, clayey silt, fine quartz sand: carbonaceous, micaceous, pyritic, burrowed, with abundant arenaceous foraminifera, minor calcareous foraminifera and shelly fossils; shallow marine (below and close to storm wave base) deposits.|
15030|Pember Mudstone|69297|5|Briefly described|p79, p98|Ypresian|Thanetian|Otway Basin. ||Wangerrip Group||Overlies the Pebble Point Formation. Overlain by the Dilwyn Formation. |Mudstone. |
15030|Pember Mudstone|69651|5|Briefly described|p10|Eocene|Paleocene|||Wangerrip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation. Abuts Eastern View Formation.||
15030|Pember Mudstone|70077|5|Briefly described|Nelson: Fig.2. Regional: Fig.4; p5, p8|Eocene|Paleocene|Otway Basin. Strongly progradational sediments. Seals the Pebble Point Formation.||Wangerrip Group.||Overlies Pebble Point Formation. Is partly equivalent to and partly overlain by Dilwyn Formation.||
15030|Pember Mudstone|70078|5|Briefly described|Northern: Fig.2. Regional: Fig.4|Eocene|Paleocene|Gambier Embayment and Voluta Trough.||Wangerrip Group.||Overlies Pebble Point Formation. Is overlain by Dilwyn Formation.||
15030|Pember Mudstone|70193|6|Mentioned|p284 Fig 2, p285 fig 3|Thanetian|Thanetian|Geological province: Otway Basin.  Part of the Sherbrook Supersequence.||||||
15030|Pember Mudstone|70880|6|Mentioned|p77|Eocene|Paleocene|Otway Basin.||||||
15030|Pember Mudstone|71266|6|Mentioned|p614 Fig.3|Eocene|Eocene|Otway Basin.||||||
15030|Pember Mudstone|73357|5|Briefly described|p25, p27, p31, p44, p46, p48|Ypressian|Thanetian|Otway Basin. Correlated with multiple biozones including Lygistepollenites balmei Spore-Pollen Zone in lower part, Malvacipollis diversus Spore-Pollen Zone in upper part; typically marginal marine depositional settings.||Of Wangerrip Group?||Overlies Pebble Point Formation, underlies Dilwyn Formation.|Includes shales.|
15030|Pember Mudstone|73383|5|Briefly described|p3, p10 Tb.3.7, p21, p24, p27, p213-214|Eocene|Paleocene|Otway Basin. Equivalent to chemostratigraphic package S5-P8 containing high Th/K, Fe and P values. Lithologies based on geochemistry using the ChemLith classification includes limestone, argillaceous and calcareous sandstones; and using the Herron classification (1988) includes wacke, shale, Fe-sand, litharenite. See also vi, p11 Tb.3.9, p82-83, p131, p258.||Wangerrip Group||Overlies Pebble Point Formation, underlies Dilwyn Formation|Sandstones, mudstones.|
15030|Pember Mudstone|73385|5|Briefly described|p5|Eocene|Paleocene|Otway Basin.||Wangerrip Group||Overlies Pebble Point Formation, underlies Dilwyn Formation.|Marginal marine and lower coastal plain sandstones, mudstones.|
15030|Pember Mudstone|73386|4|Described|p4, p6, p12, Attachment A1|Ypresian|Thanetian|Otway Basin. Unit grades to a sandier facies landwards in the onshore eastern Otway Basin. Belongs to the Upper Lygistepollenites balmei to Lower Malvacipollis diversus spore-pollen subzones, latest Thanetian to earliest Eocene in age.||Wangerrip Group||Overlies Pebble point Formation, underlies Dilwyn Formation|Shallow marine, prodelta silty claystone.|
15030|Pember Mudstone|73594|5|Briefly described|p4, p45 Fig.5.19|Eocene|Paleocene|Otway Basin.||Wangerrip Group||Overlies Pebble Point Formation, underlies Dilwyn Formation||
15136|Phi Kappa Formation|40127|6|Mentioned|p12|||||||||
15154|Piccaninny Creek Adamellite|40660|6|Mentioned|Table 5|||||||||
15154|Piccaninny Creek Adamellite|41855|4|Described|p63|||Shown as "adamellite" p10, and "granite" p51.||||||25-SEP-07
15154|Piccaninny Creek Adamellite|66174|14|Not recorded|?|||||||||
15155|Piccaninny Creek Granite|40310|6|Mentioned|Fig.1|||See Piccaninny Creek Adamellite [McClenaghan Feb95]||||||
15155|Piccaninny Creek Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite,  Blue Tier Batholith. I-type granite, mafic to felsic; unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
15155|Piccaninny Creek Granite|71730|6|Mentioned|p33, p35, p37, p56|||[Formal name intended?Name implied by table].|||||I-type granite.|
15156|Piccaninny Creek adamellite|41855|6|Mentioned|p10|||||||||
15157|Piccaninny Creek granite|22627|5|Briefly described|p134|Devonian|Devonian|||||||07-MAR-16
15157|Piccaninny Creek granite|40660|6|Mentioned|p203|||||||||
15157|Piccaninny Creek granite|41855|6|Mentioned|p51|||Same as Piccaninny Creek adamellite, p10.||||||27-SEP-07
15157|Piccaninny Creek granite|44135|6|Mentioned|p42|||Displays a north-trending tectonic foliation.||||||07-DEC-09
15158|Piccaninny Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Piccaninny Creek Adamellite or Piccaninny Point Granodiorite?||||||31-OCT-07
33484|Piccaninny Granodiorite|63171|5|Briefly described|p257||Devonian|Granodiorite pluton with trace amounts of clinopyroxene, in association with actinolite.||||||
15159|Piccaninny Point granodiorite|40660|6|Mentioned|p215|||||||||
15159|Piccaninny Point granodiorite|66575|6|Mentioned|p936 Fig.2|||Lithology not specified in figure.||||||
15165|Picnic Point quartzite|37468|6|Mentioned|Table II|||||||||
15177|Pieman Granite|22627|6|Mentioned|fig3p126|Early Carboniferous|Late Devonian|||||||
15177|Pieman Granite|30294|6|Mentioned|p862|||||||||
15177|Pieman Granite|40070|6|Mentioned|p19|||||||||
15177|Pieman Granite|42154|6|Mentioned|p339|||||||||
15177|Pieman Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
15177|Pieman Granite|44105|4|Described|p256|||Of the Pieman Suite (p259).||||||27-SEP-07
15177|Pieman Granite|44135|5|Briefly described|p12|Early Carboniferous|Early Carboniferous|Age: ca 356.5-338.5Ma. Intrudes Rocky Cape Group rocks. Petrologically similar to the white phase of Heemskirk Granite.||||||07-DEC-09
15177|Pieman Granite|61216|5|Briefly described|p32|||Small body of coarse-gr.granite:K-feldspar, plagioclase, quartz, biotite + muscovite + accessory tourmaline, zircon + apatite.Texture varies - equigran. to distinctly porphyritic, with altered perthitic K-feldspar phenocrysts.See also Pieman Head Granite||||||10-FEB-11
15177|Pieman Granite|63825|5|Briefly described|p7, p20-26|Devonian|Devonian|Geophysical interpretation of the granitoids is presented. May connect with Heemskirk Granite?  Intruded into pre-Cambrian basement rocks.||||||03-APR-08
15177|Pieman Granite|69876|5|Briefly described|p304, p313|Carboniferous|Carboniferous|Sr ratios.|~349-339 Ma (Rb-Sr). ||||S-type granite.|
73432|Pieman Group|63168|6|Mentioned|p50 Tb. 3.1|||Of Hills and Carey (1949).||||||
73647|Pieman Head (Conical Rocks) Granite|63540|5|Briefly described|Map legend||Devonian|Of Pieman Suite. One of the west  Tasmanian granites.  S-type granite, felsic; moderately to strongly fractionated, reduced. Name implied from map legend.||||||26-SEP-07
81287|Pieman Heads Granite|71100|4|Described|p125-127,130,132-135|Famennian|Famennian|Geological province: Lachlan Orogen. S-type strongly peraluminous granite. (Erroneously called Pieman Hill Granite?? p129). Crops out 20km N of Heemskirk granite. Surface exposure of ~8km2. Connected to the Interview River Granite and Sandy Cape Granite at depths of 1 km or more below the present-day surface (cf. Leaman and Richardson, 2003).|366+\-4 Ma|||Intrudes into Rocky Cape Group. Overlain by Tertiary and Quaternary cover.|Fine- to coarse-grained, and equigranular to porphyritic. Quartz, K-feldspar, plagioclase, biotite and muscovite, with accessory tourmaline, apatite, zircon, monazite and titanite, ilmenite/magnetite.|
81287|Pieman Heads Granite|71141|5|Briefly described|p125, p127, p129-p130, p132-p133, p135|||Also known as 'Conical Rocks'. Crops out 20km north of the Heemskirk Granite and has a surface area of 8km^2. Geochronology, geochemistry, mineralogy and K-feldspar Pb results are provided and discussed in detail. S-type. Overlain by Tertiary and Quaternary sedimentary rocks [not named].|365+/-4 Ma|||Intrudes the Rocky Cape Group.|Fine- to coarse-grained, and equigranular to porphyritic S-type granite composed of white K-feldspar, biotite, quartz and minor muscovite.|07-AUG-19
15238|Pine Hill Adamellite|33218|6|Mentioned|Fig.19|||||||||
15239|Pine Hill Complex|31174|4|Described|p235|||Geochemistry||||||
15241|Pine Hill Granite|22627|6|Mentioned|p132, fig8p137|Devonian|Devonian|||||||
15241|Pine Hill Granite|22711|5|Briefly described|p171|Devonian|Devonian|||||||
15241|Pine Hill Granite|23111|4|Described|p488|||||||||
15241|Pine Hill Granite|37053|4|Described|p398|||||||||
15241|Pine Hill Granite|38260|6|Mentioned|p200|||||||||
15241|Pine Hill Granite|38261|6|Mentioned|p206|||||||||
15241|Pine Hill Granite|39772|6|Mentioned|Fig.8|||||||||
15241|Pine Hill Granite|63540|5|Briefly described|Map legend||Devonian|Presented as a compound name --  Renison/Pine Hill (granites). Of the Renison Suite. One of west Tasmanian granites. I-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||26-SEP-07
15241|Pine Hill Granite|63825|6|Mentioned|p7, p130-140|Devonian|Devonian|Geophysical interpretation of the granitoids is presented.||||||03-APR-08
15241|Pine Hill Granite|64394|5|Briefly described|p98|Devonian|Devonian|Age: 355+/-4Ma (Brooks, 1966).||||||
15241|Pine Hill Granite|69872|6|Mentioned|p19|||Mentioned as part of the Heemskirk-Pine Hill-Granite Tor Granite intrusion.||||||
15241|Pine Hill Granite|69874|5|Briefly described|p127 Fig 4.27|Devonian|Devonian|Shown as (Pine Hill/Renison Granite) p127 Fig 4.26.|||||Quartz porphyry and massive quartz bodies.|
15241|Pine Hill Granite|69876|5|Briefly described|p351, 352|Devonian|Devonian|Part of an ENE-trending granite high that extends from Heemskirk Granite to Granite Tor. Also appears as Pine Hill granite. Associated tin mineralisation in Renison Bell Mine Sequence.||||Intrudes Success Creek Group, Crimson Creek Formation, Dalcoath Member.|Granite showing zonal alteration from tourmalinised greisen through sericite-rich alteration to a least-altered albite zone.|
15241|Pine Hill Granite|71100|4|Described|p124-127,129-130,132-134,136|Famennian|Famennian|Geological province: Lachlan Orogen. I-type granite. Weakly metaluminous to moderately peraluminous. Very limited exposure, but is part of an inferred E-trending sub-surface batholith at >2km depth extending from Heemskirk Granite to Granite Tor in W Tasmania. Intrudes into Success Creek Group and Crimson Creek Formation. LA-ICP-MS zircon U-Pb dating yields weighted mean age of 366.6+\-3.4/4.4 Ma, older than Rb-Sr whole rock age of 355+\-4 Ma for the porphyritic phase of the Pine Hill Granite (Brooks, 1966). Formed after Tabberabberan Orogeny (c. 390 Ma; docking of E and W Tasmanian Terranes) and ensuing crustal delamination and lithospheric upwelling. Basaltic magmatism during post-collisional extension contributed enough heat to partially melt overlying lower-crusted Proterozoic amphibolites, and to assimilate considerable amounts of upper-crusted sedimentary rocks, and after a period of protracted stagnation, resulted in felsic metaluminous I-type and peraluminous S-type granites, ranging from 374 to 360 Ma.|366+\-3 Ma||||I-type granite. Medium- to coarse-grained, locally porphyritic. |
15241|Pine Hill Granite|71141|5|Briefly described|p124-p125, p127, p129-p130, p132-p133|Upper Devonian|Upper Devonian|Very limited surface exposure, crops out 2km southeast of the Renison Bell Sn deposit. Associated with Sn-W mineralisation and formed in a post-collisional extensional margin. Geochronology, geochemistry, mineralogy and K-feldspar Pb results are provided and discussed in detail.|366 +/- 3 Ma (U-Pb date)|||Intrudes the Success Creek Group.|Moderately to strongly fractionated, medium to coarse grained, locally porphyritic, K-feldspar-biotite-quartz I-type granite.|
15241|Pine Hill Granite|71730|5|Briefly described|p7, p32, p34, p36, p39,|||Western Tasmania. Moderate mean heat generation. See also p47, p58, p60,|||||I-type granite.|
15242|Pine Hill granite|38260|6|Mentioned|p200|||||||||
15242|Pine Hill granite|39772|6|Mentioned|p18|||||||||
15242|Pine Hill granite|41141|6|Mentioned|p301|||||||||
73290|Pinnacles rhyolite|63238|6|Mentioned|p10|||Informal name - presented as Pinnacles rhyolite body, previously mapped as central Volcanic Complex lava, is now interpreted to be a correlate of the variable the Que dacites. ||||||
15280|Pioneer Beds|23949|5|Briefly described|p1123|Darriwilian|Darriwilian|Of the Owen Group.  Unconformably to disconformably overlies the rest of the Owen Group.  Conformably overlain by the Gordon Group.  Age: ~493 Ma.||||||
15280|Pioneer Beds|30278|6|Mentioned|p183|||Cross section on P183||||||
15280|Pioneer Beds|30281|5|Briefly described|p9|||||||||
15280|Pioneer Beds|31462|6|Mentioned|p379|||See also Fig.2. Ord.-Camb.||||||
15280|Pioneer Beds|32794|6|Mentioned|p608|||||||||
15280|Pioneer Beds|33218|6|Mentioned|Fig.5|||P11||||||
15280|Pioneer Beds|34298|6|Mentioned|Fig.4|||Ord.||||||
15280|Pioneer Beds|34501|6|Mentioned|p40|||Part of Owen Conglomerate. PP41,43,46||||||
15280|Pioneer Beds|34502|6|Mentioned|Fig.2|||||||||
15280|Pioneer Beds|35844|6|Mentioned|p10|||See Pioneer beds for valid name. See also p24.||||||24-MAY-07
15280|Pioneer Beds|36053|6|Mentioned|p435|||See also Fig.1.||||||
15280|Pioneer Beds|36054|6|Mentioned|p437|||||||||
15280|Pioneer Beds|36161|6|Mentioned|Fig.1|||||||||
15280|Pioneer Beds|37045|6|Mentioned|Fig.3|||||||||
15280|Pioneer Beds|37047|6|Mentioned|p248|||||||||
15280|Pioneer Beds|39892|6|Mentioned|p29|||||||||
15280|Pioneer Beds|40070|6|Mentioned|p17|||||||||
15280|Pioneer Beds|40136|5|Briefly described|p37|||||||||
15280|Pioneer Beds|40890|6|Mentioned|p47|||||||||
15280|Pioneer Beds|41695|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
15280|Pioneer Beds|41896|6|Mentioned|p25|||||||||
15280|Pioneer Beds|42170|5|Briefly described|p136|||||||||
15280|Pioneer Beds|42976|5|Briefly described|Fig.2,p267|||Same as Pioneer Beds Member of Owen Conglomerate.||||||23-NOV-06
15280|Pioneer Beds|43244|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Should read Pioneer beds. Of Owen Conglomerate.||||||
15280|Pioneer Beds|43250|6|Mentioned|Map Legend|Ordovician|Cambrian|Of Owen Conglomerate. Grey to pink quartz sandstone and granule-pebble conglomerate with detrital chert clasts; fossils and chromite-rich bands in places.||||||24-MAY-07
15280|Pioneer Beds|43668|5|Briefly described|p9||Early Ordovician|||||||
15280|Pioneer Beds|43777|5|Briefly described|p4||Ordovician|||||||
15280|Pioneer Beds|44135|5|Briefly described|p19, p27|Middle Ordovician|Early Ordovician|Of Upper Owen Sandstone. Overlain by Gordon Group limestone via a thin seq. of calcareous siltstone and sandstone. Chert-rich granule-pebble conglomerate + detrital chromite in places, passing up into grey sandstone with pipestem burrows and minor shale.||||||07-DEC-09
15280|Pioneer Beds|61412|6|Mentioned|p9.||Middle Ordovician|||||||
15280|Pioneer Beds|63240|6|Mentioned|p3|||||||||
15280|Pioneer Beds|69857|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Gordon Group.|||Shallow-marine sandstone-mudstone +/- conglomerate +/- limestone; Ordovician fossils and trace fossils in places.|
15280|Pioneer Beds|69859|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Gordon Group.|||Shallow-marine sandstone-, mudstone +/- conglomerate +/- limestone sequences; Ordovician fossils and trace fossils in places.|
15280|Pioneer Beds|69876|6|Mentioned|p294|||Mt Lyell area. Regional cross-section. Appears as Owen Group (incl. Pioneer Beds).||||||
15280|Pioneer Beds|73313|6|Mentioned|Map legend|Ordovician|Furongian|Map unit includes Moina Sandstone, Pioneer Beds. Description of shallow marine sandstone-mudstone +/- conglomerate +/- limestone; Ordovician fossils and trace fossils in places. Unconformity on older rocks in places.||Gordon Group||||
15280|Pioneer Beds|73320|6|Mentioned|Map legend|Ordovician|Ordovician|Western Tasmania. Map unit includes Moina Sandstone, Pioneer Beds, Butler Island Formation; description of shallow marine sandstone-mudstone +/- conglomerate +/- limestone sequences, typically grey. Ordovician fossils and trace fossils in places.||Gordon Group||||
29622|Pioneer Beds Member|42976|5|Briefly described|p267|||Of Owen Conglomerate???||||||15-OCT-07
40529|Pioneer Beds, Lower|23948|6|Mentioned|p1091 Fig.1|Ordovician|Ordovician|Informal name.||||||15-OCT-07
40524|Pioneer Beds, Upper|23948|6|Mentioned|p1091 Fig.1|Ordovician|Ordovician|Informal name.||||||15-OCT-07
83508|Pioneer Group|73489|6|Mentioned|p661|||See also Pioneer Sandstone.||||||
28929|Pioneer beds|638|5|Briefly described|p88 Fig. 4.2|Ordovician|Ordovician|Of the Gordon Group. ||||||
28929|Pioneer beds|22627|6|Mentioned|p132|Ordovician|Late Cambrian|||||||
28929|Pioneer beds|35844|6|Mentioned|Fig.12|||See also Pioneer Beds.||||||24-MAY-07
28929|Pioneer beds|43164|6|Mentioned|23||Cambrian|||||||
28929|Pioneer beds|63169|5|Briefly described|p157 Fig. 5.2, p164|Ordovician|Early Ordovician|Form the uppermost part of the Owen sequence. Truncates the Tyndall Group and overlaps onto the Darwin Granite at South Darwin Peak. Thickness: ~10m. Geological Province: Dundas Trough.||||||31-OCT-07
28929|Pioneer beds|69875|6|Mentioned|p246|||Wade and Solomon (1958). Later the Pioneer Sandstone of Corbett (2001).||||||
15355|Poets Road Siltstone|35280|6|Mentioned|p144|||||||||
15354|Poets Road Siltstone Member|35280|6|Mentioned|p144|||||||||
15356|Poets Road member|35280|6|Mentioned|p145|||||||||
15358|Poimena Adamellite|35826|6|Mentioned|Fig.21|||||||||
15358|Poimena Adamellite|61216|6|Mentioned|p45|||Same unit as Poimena Granite - unclear which name is current. Overlies Lottah Granite.||||||10-FEB-11
77661|Poimena Pluton|67804|5|Briefly described|p69|Middle Devonian|Middle Devonian|[The word Pluton is being used as a synonym for the Granite]|384 +/- 3 Ma.|||Intrudes Mathinna Supergroup.||
15360|Poimena adamellite|39927|6|Mentioned|p305|||||||||
15361|Poimena biotite adamellite|39927|6|Mentioned|p311|||||||||
15362|Poimena biotite granite|37797|6|Mentioned|p141|||||||||
15363|Poimena granite|37797|6|Mentioned|p139|||||||||
15372|Point Hibbs Limestone|31502|5|Briefly described|p95|||Devonian corals. Early Siegenian||||||
15372|Point Hibbs Limestone|31503|6|Mentioned|p1|||Fauna. Siegenian - Lower Couvinian.||||||
15372|Point Hibbs Limestone|32619|6|Mentioned|p464|||Siegenian to early Emsian||||||
15372|Point Hibbs Limestone|33326|6|Mentioned|p434|||Fauna.||||||
15372|Point Hibbs Limestone|33732|4|Described|p109|||Of Spero Bay Group.||||||
15372|Point Hibbs Limestone|33839|6|Mentioned|p576|||||||||
15372|Point Hibbs Limestone|34189|6|Mentioned|p5|||Faunal similarities.||||||
15372|Point Hibbs Limestone|41317|4|Described|p172|||Defines the Point Hibbs Formation to replace the Point Hibbs Limestone.||||||
15372|Point Hibbs Limestone|42799|5|Briefly described|p64|||||||||
15372|Point Hibbs Limestone|43530|14|Not recorded|p1027,1028||Siegenian|Part of Spero Bay Group||||||
15372|Point Hibbs Limestone|43547|14|Not recorded|Tb p158,159,160||Emsian|Part of Spero Bay Group||||||
15372|Point Hibbs Limestone|48846|14|Not recorded|p12|||||||||
15372|Point Hibbs Limestone|63120|6|Mentioned|p217|Early Devonian|Early Devonian|||||||
15372|Point Hibbs Limestone|63170|5|Briefly described|p210, p225 Fig. 6.12, p229|Pragian|Pragian|Of Banks (1962e, 1970a). Of Spero Bay Group. Overlain by Red Reef Cliff  Sandstone. Thickness: <180m. In the Western Tasmania Terrane. Interbedded limestone and calcareous mudstone with abundant coral; limestone is thinly bedded fossiliferous packstone.||||||07-FEB-11
15372|Point Hibbs Limestone|68297|5|Briefly described|p184, 191|Pragian|Lochkovian|Tas. Includes possible shark scales.||||||
15372|Point Hibbs Limestone|69875|4|Described|p258-259, p262|Pragian|Pragian|<180m thick. Age determined from Fig 5.13. Fauna (listed) probably the same age as Bell Shale. See reference to Point Hibbs Formation, also on p262. Open marine deposits.||Basal Spero Bay Group||Underlies Red Reef Cliff Siltstone conformably.|Diversely fossiliferous lime packstone interbedded with calcareous terrigenous mudstone.|
15371|Point Hibbs Limestone""|41317|6|Mentioned|p175|||||||||
79564|Pontoon Hill Member|69875|5|Briefly described|p243 Fig 5.2|Early Ordovician|Early Ordovician|Fossil control.||Florentine Valley Formation||Underlies Mount Field Member. Overlies Churchill Sandstone Member.||
15427|Pontoon Hill Siltstone|40136|6|Mentioned|p24|||||||||
15451|Porcupine Creek Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Porcupine Creek Granodiorite [M.McClenaghan Jan95]||||||
15451|Porcupine Creek Granite|61216|5|Briefly described|p20 Fig. 7a|||Presented as Porcupine Creek only in map of granites. Part of the Scottsdale Batholith.||||||10-FEB-11
15451|Porcupine Creek Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Diddleum Suite, Scottsdale Batholith.  I-type granite, mafic, unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
69174|Port Campbell Limestone Formation|60538|5|Briefly described|p471 Fig. 10|||||||||
15463|Port Campbell limestone|23909|5|Briefly described|p290|||Informal - see Port Campbell Limestone.  Geological Province: Otway Basin.||||||
15463|Port Campbell limestone|24551|5|Briefly described|p246|Miocene|Miocene|Of the Heytesbury Group.||||||
15463|Port Campbell limestone|35066|3|Fully described|p212|||||||||
73652|Port Cygnet Granite|63540|5|Briefly described|Map legend|Cretaceous|Cretaceous|An alkaline intrusive - I-type granite, mafic; unfractionated, oxidised. Name implied from map legend.||||||26-SEP-07
15466|Port Cygnet trachyte|40811|6|Mentioned|p327|||||||||
15481|Port Slate and Quartzite|42358|5|Briefly described|p19|||Used by Spry 1957. Discussed under Detention Subgroup.||||||
81325|Port Sorell Group|70025|5|Briefly described|p4-5|Ediacaran|Cryogenian|Sorrell-Badger Head Zone. Abbreviated as PS on p4 Fig 2.|||||Sandstone, mudstone and dolomite, with rift-related mafic volcanic rocks.|
34170|Port Sorell Sequence|22627|6|Mentioned|p128|Cambrian|Cambrian|||||||
74075|Port Sorrell basalts|61395|6|Mentioned|p92|||Informal reference to basalts of the Port Sorrell Formation.||||||07-FEB-11
31034|Porter's Hill beds""|43474|14|Not recorded|p59|||See also Lexicon. Of Johnston 1888 et seq. Probably Late Sakmarian. Part of Bundella Mudstone.||||||
31933|Porter's Hill mudstone|43876|14|Not recorded|p587||Permian|||||||
15490|Porters Hill Mudstone|31706|6|Mentioned|p671|||Correlation chart of Gondwana System||||||
79501|Powena Beds|69874|4|Described|p149, p214-216, p238-239|Furongian|Furongian|South Coast area, near New River Lagoon. Contains a rich trilobite fauna of late Iverian age. Probably equivalent to the basal part of Wierah Formation.||||Underlies Wierah Formation conformably. Overlies Point Vivian Formation unconformably? Equivalent to lower part of Wierah Formation.|A fault-bounded block of fossiliferous calcareous siltstone and sandstone.|
79501|Powena Beds|70753|5|Briefly described|p184, p190|Late Cambrian|Late Cambrian|Bischoff (1983){BSc (hons)). Cecil Fault Zone. 15m thick. Fossils (agnostoid and trilobite) in the carbonate unit are listed, and Iverian age-related anomalies discussed. Possibly equivalent to basal Wierah Formation.|||||Laminated fine quartz wacke and dolomitic quartz wacke (3m), overlain by thin-bedded and nodular fossiliferous calcilutite and calcareous siltstone (10m), capped by massive sandstone (2m).|21-NOV-16
15545|Precipitous Bluff Beds|37408|4|Described|p97|||Reserved as Precipitous Bluff.||||||
15545|Precipitous Bluff Beds|42478|6|Mentioned|p1|||Also p25.||||||27-SEP-07
15545|Precipitous Bluff Beds|69875|5|Briefly described|p254, p257, p271|||Deposited in deep subtidal environment. Fauna and corals described, indicate reef facies. Possible reservoir for hydrocarbons.||||Correlated with Benjamin Limestone. Overlies New River Beds.|Basal unit of argillaceous limestone contains conodonts, 4m fossiliferous buff siltstone with brachiopods, then 230m siltstone and calcareous shale with minor interbedded micrite and calcarenite; conodonts half way up.|
15548|Preolenna Coal Measure|30325|6|Mentioned|p123|||||||||
15548|Preolenna Coal Measure|41911|6|Mentioned|p164|||||||||
15548|Preolenna Coal Measure|42185|6|Mentioned|p365|||||||||
15560|Pretty Hill Sandstone|22875|5|Briefly described|p26 Table1|||||||||
15560|Pretty Hill Sandstone|24056|4|Described|p84|Early Cretaceous|Early Cretaceous|Of Otway Group.  Max. thickness: 1590m.  Geological Basin: Otway Basin.||||||
15560|Pretty Hill Sandstone|24208|5|Briefly described|p169, p180|Early Cretaceous|Early Cretaceous|Of the Crayfish Group. Geological Province: Penola Trough (Otway Basin).||||||05-FEB-08
15560|Pretty Hill Sandstone|24209|6|Mentioned|p151|||Informally named by Lovibond et al (1995).||||||
15560|Pretty Hill Sandstone|24551|5|Briefly described|p242|Early Cretaceous|Late Jurassic|Of the Otway Basin.||||||
15560|Pretty Hill Sandstone|24562|5|Briefly described|p3 Table 1|||Geological Province: Otway Basin.||||||
15560|Pretty Hill Sandstone|30578|5|Briefly described|p5|||||||||
15560|Pretty Hill Sandstone|30905|6|Mentioned|Table 7.3|||||||||
15560|Pretty Hill Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
15560|Pretty Hill Sandstone|33940|6|Mentioned|Fig.21-1|||Neocomian.||||||
15560|Pretty Hill Sandstone|35013|5|Briefly described|p390|||||||||
15560|Pretty Hill Sandstone|38625|6|Mentioned|Table 2|||||||||
15560|Pretty Hill Sandstone|39315|6|Mentioned|Fig.7|||||||||
15560|Pretty Hill Sandstone|40560|6|Mentioned|p4|||||||||
15560|Pretty Hill Sandstone|41016|5|Briefly described|p214|||||||||
15560|Pretty Hill Sandstone|41185|5|Briefly described|p177|||||||||
15560|Pretty Hill Sandstone|41454|6|Mentioned|p61|||||||||
15560|Pretty Hill Sandstone|41704|6|Mentioned|p99|||||||||
15560|Pretty Hill Sandstone|41726|5|Briefly described|p420|||See also p425.||||||18-FEB-08
15560|Pretty Hill Sandstone|41769|6|Mentioned|p57|||||||||
15560|Pretty Hill Sandstone|41868|4|Described|p531|||||||||
15560|Pretty Hill Sandstone|41936|6|Mentioned|p77|||||||||
15560|Pretty Hill Sandstone|42152|4|Described|p10|||See also p39.||||||18-FEB-08
15560|Pretty Hill Sandstone|42318|6|Mentioned|Fig.5 P12|||||||||
15560|Pretty Hill Sandstone|42361|3|Fully described|p4|Neocomian||||||||
15560|Pretty Hill Sandstone|42524|4|Described|p27|||||||||
15560|Pretty Hill Sandstone|42545|6|Mentioned|p18|||Otway Basin.||||||
15560|Pretty Hill Sandstone|42555|5|Briefly described|Fig.2 P285|||||||||
15560|Pretty Hill Sandstone|42599|5|Briefly described|Fig.3 P614|||||||||
15560|Pretty Hill Sandstone|42827|5|Briefly described|p218|||||||||
15560|Pretty Hill Sandstone|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
15560|Pretty Hill Sandstone|43171|6|Mentioned|8|||Of Crayfish Group. Age: 135-145 Ma||||||
15560|Pretty Hill Sandstone|43208|5|Briefly described|map legend|Aptian|Valanginian|Of Otway Group.||||||
15560|Pretty Hill Sandstone|43590|4|Described|p9|Aptian|Valanginian|||||||
15560|Pretty Hill Sandstone|43660|5|Briefly described|p14|||||||||
15560|Pretty Hill Sandstone|43709|6|Mentioned|p10||Early Cretaceous|||||||
15560|Pretty Hill Sandstone|43711|6|Mentioned|p21||Early Cretaceous|||||||
15560|Pretty Hill Sandstone|43733|6|Mentioned|Fig.2.11,p65||Early Cretaceous|||||||
15560|Pretty Hill Sandstone|43747|5|Briefly described|p5||Early Cretaceous|||||||
15560|Pretty Hill Sandstone|43784|6|Mentioned|p28|||||||||
15560|Pretty Hill Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
15560|Pretty Hill Sandstone|61182|5|Briefly described|p12|||Fine-gr.sediments and sandstone included in Crayfish Fm by some authors eg. Sprigg (1986); or in Crayfish Group by Kopsen and Scholefield (1990) and in Crayfish Subgroup by Morton (1990). Pretty Hill Fm is preferred for the predominantly sandstone unit.||||||
15560|Pretty Hill Sandstone|61329|6|Mentioned|p121|||Geological Province: Otway Basin.||||||
15560|Pretty Hill Sandstone|61547|5|Briefly described|p459, p460 Fig.1, pp463-46, p467 Fig.7.|Early Cretaceous|Early Cretaceous|Hydrocarbon reservoir in the Penola Trough, Otway Basin. Juxtaposed against the Katnook Sandstone across the Pyrus Fault, allowing leakage. This is not the case with the Ladbroke Grove fault. Deposited in a braided fluvial environment.||Unit in Pretty Hill Formation.||Overlies Casterton Formation.|Massive, slumped and cross-bedded sand packages: litharenite to feldspathic litharenite.|
15560|Pretty Hill Sandstone|61618|6|Mentioned|p431|||Misspelt name.||||||
15560|Pretty Hill Sandstone|63124|5|Briefly described|p48 Fig. 5.1, p58-59|||Of Morton (1990). Re-introduced in 1995 (Lovibond et al) as member of Pretty Hill Formation - contradicting International Strat. Guide conventions and used without proper definition. Now invalid. Geological Province: Otway Basin.||||||31-JAN-08
15560|Pretty Hill Sandstone|63129|6|Mentioned|p131, p132|||Probably misspelt and should be Pretty Hill Formation. Geological Province: Otway Basin.||||||30-JAN-08
15560|Pretty Hill Sandstone|63267|6|Mentioned|p488-490, p492-495|Early Cretaceous|Early Cretaceous|Used apparently interchangeably (even within the same sentence!) as Pretty Hill Formation (see references p483-486, p491-493, p495-497).||||||
15560|Pretty Hill Sandstone|63431|5|Briefly described|p677 Fig. 2||Berriasian|Appears to be the basal section of the Pretty Hill Formation - a formal name is probably not intended?||||||07-FEB-11
15560|Pretty Hill Sandstone|67061|6|Mentioned|p546 Fig.3.|Aptian|Aptian|||Unit in Otway Group.||||
15560|Pretty Hill Sandstone|72050|6|Mentioned|p237|||Otway Basin. First penetrated in 1962 at Pretty Hill-1; showed high porosity and permeability. Later drilling met with minor hydrocarbon shows.||||||
15560|Pretty Hill Sandstone|73356|6|Mentioned|p4-5, p20|||Of Reynolds et al. (1966). Abandoned name. [Also written as 'Pretty Hill Sandstone']. [See Pretty Hill Formation].||||||
15560|Pretty Hill Sandstone|73383|6|Mentioned|p15, p153-156, p278-281|||Otway Basin. Informal lithology-based unit. Lithologies based on geochemistry using the ChemLith classification includes sandstone, argillaceous sandstone, mudstone, limestone and calcareous limestone; and using the Herron classification (1988) includes shale, Fe-sand, Fe-shale, wacke, lith-arenite and sublith-arenite. See also Pretty Hill Formation.||Pretty Hill Formation||||
15560|Pretty Hill Sandstone|73594|5|Briefly described|p14, p45, p51|||Otway Basin. Name retained by Lovibond et al. (1995) as the uppermost informal unit of the Pretty Hill Formation.||Pretty Hill Formation, upper part||Overlies Upper Sawpit Shale, underlies Laira Formation||
73291|Primrose Piroclastics""|63238|5|Briefly described|p20 Fig. 3|||Misspelt - see "Primrose Pyroclastics". ||||||
28941|Primrose Pyroclastics and Slate""|40890|5|Briefly described|p51|||||||||
73275|Primrose Pyroclastics""|638|5|Briefly described|p92|||Of Brathwaite (1974). Partly included in the Rosebery-Hercules Pyroclastic Sequence.||||||
73275|Primrose Pyroclastics""|63238|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Informal name for upper part of White Spur Formation at Rosebery - in part reassigned and correlated with Tyndall Group. Underlies Stitt Quartzite. See also p22. Misspelt as "Primrose Piroclastics in Fig. 3, p20. ||||||
73275|Primrose Pyroclastics""|63240|5|Briefly described|p4|||Now part of White Spur Formation in the curve of Rosebery Fault - redesignated as Tyndall Group -- and overlain by Stitt Quartzite.||||||14-MAY-07
15584|Primrose Volcanics|29930|6|Mentioned|p1086|||||||||
15585|Primrose pyroclastics|37044|6|Mentioned|Fig.8|||||||||
15586|Primrose tuffs|37049|6|Mentioned|p307|||||||||
24463|Prion Beach Beds|13995|5|Briefly described|p85|||Trilobite species named.|||||Peri-platform micrites.|
24463|Prion Beach Beds|37408|4|Described|p97|||||||||
24463|Prion Beach Beds|40714|5|Briefly described|Fig.2|||||||||
24463|Prion Beach Beds|42478|6|Mentioned|p1, p5|||||||||
24463|Prion Beach Beds|69875|5|Briefly described|p254|Eastonian|Gisbornian|Eastern end of Prion Beach and on the Isle du Golfe.||||Correlate with Benjamin Limestone.  |Thin-bedded argilliceous limestone; trilobites, brachiopods, conodonts.|
15607|Priory Monzonite|35826|3|Fully described|p129|||||||||
15607|Priory Monzonite|35827|4|Described|p27|||||||||
73292|Professor Range Sequence|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Late Cambrian|Probably an informal name - probably(?) refers to upper part of "Rosebery Group" in the Rosebery-White Spur area. Underlain by Higgins Creek Sequence.||||||
15654|Pumphouse lava and central volcanics|39892|6|Mentioned|Table 2|||||||||
25418|Pumphouse rhyodacite|39892|6|Mentioned|p32|||||||||
23924|Puncheon Point granite|36374|3|Fully described|p58|||||||||
15696|Pyengana Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Pyengana Granodiorite.||||||
15696|Pyengana Granite|61216|5|Briefly described|p20 Fig. 7a|||Presented as Pyengana only in map of granites. Part of the Blue Tier Batholith.||||||10-FEB-11
15696|Pyengana Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith. I-type granite, mafic; unfractionated, oxidised. Name implied from map legend.||||||
15696|Pyengana Granite|71730|6|Mentioned|p33, p35, p37, p56||||||||I-type granite.|
34173|Pyengana Pluton|22627|6|Mentioned|p132|||||||||
15698|Pyengana granodiorite|23467|5|Briefly described|p282|||||||||
15698|Pyengana granodiorite|37797|6|Mentioned|p139|||||||||
15716|Quambi Group|34287|6|Mentioned|p129|||Misspelling of Quamby Group, Tas [CEBMar95]||||||
25424|Quamby Formation|24547|6|Mentioned|p3 preface|||See Quamby Mudstone. Of Wells (1957), but elevated to Group status by McKellar (1957)||||||10-MAY-04
25424|Quamby Formation|24549|4|Described|p9|Permian|Permian|Of the Golden Valley Group. Max Thickness: 330ft. Uniform and massive dark grey mica mudstone||||||07-FEB-08
25424|Quamby Formation|24552|4|Described|p7||Late Carboniferous|Poorly fossiliferous massive bedded pyritic, carbonaceous, glendonitic mudstone and siltstone. Geological Province: Tasmanian Basin. See also Quamby Group.||||||07-FEB-11
25424|Quamby Formation|30819|6|Mentioned|p107|||||||||
25424|Quamby Formation|33492|6|Mentioned|p18|||Permian||||||
25424|Quamby Formation|34316|5|Briefly described|p21 Fig.3|Early Permian|Early Permian|Of the Golden Valley Group.  Dark grey mica mudstone.||||||06-FEB-08
25424|Quamby Formation|36788|6|Mentioned|p104|||||||||
25424|Quamby Formation|39579|6|Mentioned|p13|||See also P19||||||
25424|Quamby Formation|41896|6|Mentioned|p33|||||||||
25424|Quamby Formation|42000|6|Mentioned|p53|||||||||
25424|Quamby Formation|43022|6|Mentioned|p472|||||||||
25424|Quamby Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Beckers Formation, Lochinvar Formation, Wasp Head Formation and Woody Island Formation. Geological Province: Tasmanian Basin.||||||
25424|Quamby Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Early Permian|Informal - see Quamby Mudstone.||||||07-FEB-11
25424|Quamby Formation|67543|6|Mentioned|p145 Fig.4|||Fig.4 suggests correlation with Woody Island and Inglis Formations.||||||
25424|Quamby Formation|69877|5|Briefly described|p366-367|Permian|Permian|||||Correlative with Woody Island Formation.|Dark, organic, poorly sorted, fine- to medium-grained siltstone; contains dropstones, glendonites, rare marine fossils; lightly bioturbated.|
25424|Quamby Formation|70194|6|Mentioned|p299 Fig 2|Early Permian|Late Carboniferous|||Of Parmeener Supergroup.||Laterally equivalent to Woody Island Formation. Underlain by Wynyard - Truro Formations.|Black shale.|
25424|Quamby Formation|73639|5|Briefly described|p6, 10-12, 15, 18|Permian|Permian|Sedimentological log from Ross 1 drillhole. Open-marine, post-glacial deposits; depositional setting discussed.||||Overlies Stockers Tillite.|Contains marine fossils and bioturbation at the base of the Formation.|
15718|Quamby Group|24547|6|Mentioned|p14|Permian|Permian|Informal name - referring to Quamby Mudstone, consisting of a monotonous sequence dark carbonaceous mudstone.||||||11-APR-05
15718|Quamby Group|24552|5|Briefly described|p5 Fig.2|Asselian|Asselian|Conformably overlies Stockers Tillite; conformably overlain by Golden Valley Group. Geological Province: Tasmanian Basin. See also Quamby Formation.||||||07-FEB-11
15718|Quamby Group|31251|6|Mentioned|p73|||Refers Ludbrook (1956, 1965)||||||
15718|Quamby Group|31461|6|Mentioned|p49|||||||||
15718|Quamby Group|31761|6|Mentioned|p9|||||||||
15718|Quamby Group|31855|6|Mentioned|p12|||Occurrences of oil shale||||||
15718|Quamby Group|32943|6|Mentioned|p96|||See also p106.||||||07-FEB-08
15718|Quamby Group|32945|6|Mentioned|p75|Permian|Permian|See also pp85,86 and 87.||||||07-FEB-08
15718|Quamby Group|33292|6|Mentioned|Fig.18|||||||||
15718|Quamby Group|33494|6|Mentioned|p45|||||||||
15718|Quamby Group|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
15718|Quamby Group|36110|6|Mentioned|p54|||||||||
15718|Quamby Group|37065|5|Briefly described|p29|||||||||
15718|Quamby Group|38200|6|Mentioned|p75|||||||||
15718|Quamby Group|39754|6|Mentioned|p1689|||||||||
15718|Quamby Group|41317|6|Mentioned|p172|||||||||
15718|Quamby Group|43474|14|Not recorded|p25,37,55|||||||||
15718|Quamby Group|45097|6|Mentioned|p27|||Microflora. Correlation chart||||||
15718|Quamby Group|48770|6|Mentioned|p110|||||||||
40983|Quamby Mudstone, Upper|24547|6|Mentioned|p3 preface|||Informal name - see Quamby Mudstone.||||||10-MAY-04
15721|Quamby Siltstone|30889|6|Mentioned|p46|||||||||
15721|Quamby Siltstone|70096|6|Mentioned|p221;Supp6|||See also supplementary files in appendix for additional stratigraphic and locality information.||||Overlain by Bundella Mudstone.||
15723|Quamby"" Formation|30889|6|Mentioned|p47|||||||||
15724|Quamby"" Group|30889|6|Mentioned|p47|||||||||
26116|Que River Beds|30876|2|Defined|p761|Middle Cambrian|Middle Cambrian|See also p762, p763.||||||02-OCT-07
26116|Que River Beds|31462|6|Mentioned|p379|||||||||
26116|Que River Beds|31465|6|Mentioned|p406|||Refers Trilobite content||||||
26116|Que River Beds|31473|6|Mentioned|p41|||||||||
26116|Que River Beds|32744|5|Briefly described|p177|||Fauna. Cambrian||||||
26116|Que River Beds|32745|6|Mentioned|p22|||Fauna||||||
26116|Que River Beds|35791|6|Mentioned|Fig.2|||Middle & Late Cambrian correlation chart for Tas.||||||
26116|Que River Beds|35998|6|Mentioned|p698|||||||||
26116|Que River Beds|36788|6|Mentioned|Fig.21|||||||||
26116|Que River Beds|36817|4|Described|p121|||||||||
26116|Que River Beds|39134|6|Mentioned|p195|||||||||
26116|Que River Beds|39892|6|Mentioned|p27|||||||||
26116|Que River Beds|40760|4|Described|p170|||||||||
26116|Que River Beds|41795|6|Mentioned|p53|||||||||
26116|Que River Beds|43136|5|Briefly described|p668,Fig.1.|||Misspelling/variation of Que River Shale.||||||
26116|Que River Beds|43137|5|Briefly described|Fig.1,p688|||Misspelling/variation on Que River Shale.||||||
26116|Que River Beds|62790|6|Mentioned|p208|Middle Cambrian|Middle Cambrian|Undillan. Northwest Tasmania. Contained an internal mould of a possible left valve described (Jago 1977) as bradoriid gen. et sp. indet. associated with agnostid fauna.||||||
26116|Que River Beds|69573|6|Mentioned|p654, 659, 665-666|Cambrian|Cambrian|Deeper water, outer shelf environment with low oxygen conditions. Agnostid faunas studied; complete absence of trilobites.||||||
73433|Que River Formation|63168|6|Mentioned|p48, p79|Middle Cambrian|Middle Cambrian|||||||
15737|Que River Mine dacitic volcanics|39892|6|Mentioned|p19|||Que River has been used for sedimentary units.||||||
15738|Que River Mine volcanics|39892|6|Mentioned|Table 4|||Que River has been used for sedimentary units.||||||
15740|Que River Suite|42209|6|Mentioned|Fig.4 P269|||||||||
25425|Que River beds|36788|6|Mentioned|Fig.22|||||||||
25425|Que River beds|63168|5|Briefly described|p75 Fig. 3.10|Middle Cambrian|Middle Cambrian|||||||
15741|Que River shale|638|4|Described|p88 Fig. 4.2, p102|Middle Cambrian|Middle Cambrian|Informal name. Of the Dundas Group. Conformably overlies (blankets) the Que-Hellyer Volcanics. Max. thickness: 300m. Extensive unit of pyritic black shale with interbedded siltstone and minor greywacke; contains fossils of late Middle Cambrian age.||||||
15741|Que River shale|39134|6|Mentioned|p195|||||||||
15741|Que River shale|40890|6|Mentioned|Fig.3|||||||||
73277|Que dacite|63238|5|Briefly described|p19 Fig. 2|||Informal name for rocks in the Que-Hellyer area.||||||
73277|Que dacite|63240|6|Mentioned|p5|||||||||14-MAY-07
73293|Que dacites|63238|6|Mentioned|p10|||Informal name for rocks in the Que-Hellyer area.||||||
73293|Que dacites|69874|4|Described|p150, p158-159, p161|Middle Cambrian|Middle Cambrian|Informal name. Also referred to here as Mixed Sequence. Burns Peak. Contains VHMS deposits.||Que-Hellyer Volcanics.||Underlies Southwell Subgroup. Overlies Hollway Andesites, Animal Creek Greywacke. Interbedded with Que-Hellyer Volcanics.|Dacites and volcaniclastics; contains VHMS deposits.|
73294|Que footwall andesites|63238|6|Mentioned|p10|||Informal name describing the Holloway Andesite in the Que-Hellyer area.||||||
73294|Que footwall andesites|69874|5|Briefly described|p161, p164, p179|||Informal. Also referred to here as Lower Andesites and Basalts. Up to 600m thick near the Que River mine.||Que-Hellyer Volcanics.||||
73807|Que-Hellyer "dacites"|638|6|Mentioned|p111 Fig. 4.9, p113|||Informal refernce to dacitic rocks of the Que-Hellyer Volcanics.||||||05-FEB-08
73731|Que-Hellyer footwall andesites|63612|6|Mentioned|p9|||Informal name. Intrudes the Eastern Quartz-Phyric Sequence.||||||07-FEB-11
40337|Que-Hellyer volcanics|23940|6|Mentioned|p916 Fig. 2|||Informal-see Que-Hellyer Volcanics.||||||15-JUL-15
40337|Que-Hellyer volcanics|64395|6|Mentioned|p168, p172|||Informal name of Crawford et al (1992) - see Que-Hellyer Volcanics.||||||07-FEB-11
40503|Que-River Shale|23945|5|Briefly described|p1038|||Misspelt - see Que River Shale.||||||16-JUN-09
73730|Que-hellyer complex|63612|6|Mentioned|p26|||Not intended as a formal name.||||||07-FEB-11
15750|Queenstown Limestone""|40136|6|Mentioned|p39|||||||||
34035|Queenstown Porphyry|22603|6|Mentioned|p96||Cambrian|Possibly not a formal name - may be informal description? Age: 540 Ma (?).||||||02-OCT-07
15752|Queenstown Pyroclastics|30278|6|Mentioned|p187|||Cambrian age||||||
15752|Queenstown Pyroclastics|32794|5|Briefly described|p606|||||||||
15752|Queenstown Pyroclastics|33218|6|Mentioned|Fig.5|||||||||
15752|Queenstown Pyroclastics|35092|6|Mentioned|p108|||||||||
15753|Queenstown pyroclastics|33839|5|Briefly described|p571|||||||||
15786|Radford Creek Group|35288|6|Mentioned|p12|||Misspelling of Radfords Creek?||||||
15786|Radford Creek Group|42891|5|Briefly described|Fig.3 P300|||||||||
15786|Radford Creek Group|44135|6|Mentioned|p30|||Misspelt - see Radfords Creek Group.||||||07-DEC-09
15786|Radford Creek Group|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Geological Province: Dial Range Trough.||||||22-JAN-08
15787|Radford Mudstone|42891|6|Mentioned|p298|||Variation on Radfords Creek Group?||||||
83239|Ragged Basin Complex""|73320|6|Mentioned|Map legend|Cambrian Series 2|Terreneuvian|Adamsfield - Jubilee region. Included in map unit of feldspathic and quartz-rich lithicwacke, mudstone and chert sequences with Luina Group and correlates. Considered allochthonous. Uncertainty indicated for Terreneuvian age.||||Correlate of Luina Group.||
15829|Ranelagh alkali basalt|41895|6|Mentioned|p80|||||||||
78553|Rapid River Dolomite|67502|6|Mentioned|p43, 46|||Redundant, see the Black River Dolomite. Used by McNeill (1961) and Matthews (1961) for dolomite, chert, cherty slate and breccia occurring in the Arthur River area (the Black River Dolomite as described in this report). Also shortened to Rapid Dolomite on p43,46.||||||07-JAN-15
15846|Rapid River dolomites|38638|6|Mentioned|p1902|||||||||
15906|Razorback Conglomerate|638|5|Briefly described|p88 Fig. 4.2|Middle Cambrian|Middle Cambrian|Of the Dundas Group. ||||||
15906|Razorback Conglomerate|31464|6|Mentioned|Fig.2|||Correlation chart||||||
15906|Razorback Conglomerate|33989|6|Mentioned|p496|||Cambrian||||||
15906|Razorback Conglomerate|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tasmania. See also p224.||||||21-MAY-07
15906|Razorback Conglomerate|40890|6|Mentioned|p53|||||||||
15906|Razorback Conglomerate|41795|3|Fully described|p41, Fig. 13|Middle Cambrian|Middle Cambrian|See also p46.||||||02-APR-07
15906|Razorback Conglomerate|41814|6|Mentioned|Map legend|Cambrian||||||||
15906|Razorback Conglomerate|42608|6|Mentioned|P 59|||||||||
15906|Razorback Conglomerate|43131|6|Mentioned|Fig.9,p582|||||||||
15906|Razorback Conglomerate|43191|6|Mentioned|p46|||Of Dundas Group.||||||21-MAY-07
15906|Razorback Conglomerate|43777|5|Briefly described|p2||Cambrian|||||||
15906|Razorback Conglomerate|44135|5|Briefly described|p18|||Near top of the Lower Dundas Group.||||||07-DEC-09
15906|Razorback Conglomerate|63168|4|Described|p65, p75 Fig. 3.10, p76|Middle Cambrian|Middle Cambrian|Of Dundas Group. Conformable over Red Lead Conglomerate; overlain gradationally by Brewery Junction Formation. Well-bedded sequence of grey, green and greyish-white, turbiditic, chert-clast conglomerate with interbedded siliceous sandstone and siltstone. ||||||
15906|Razorback Conglomerate|63169|5|Briefly described|p179|||Of the Dundas Group. Overlies Hodge Slate. Contains abundant chert detritus and rounded quartzite cobbles and boulders. ||||||
15906|Razorback Conglomerate|63238|5|Briefly described|p13, p18|Middle Cambrian|Middle Cambrian|Overlain by Brewery Junction Formation. Felsic volcaniclastic rocks; unfossiliferous unit. See also p20 Fig. 3.||||||
15906|Razorback Conglomerate|63240|5|Briefly described|p4|||Formerly of the "lower Dundas Group" (upper section) now redesignated, along with the lower Brewery Junction Formation, as Tyndall Group.||||||09-JUL-15
15906|Razorback Conglomerate|64395|5|Briefly described|p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Of the Dundas Group (lower part).||||||07-FEB-11
15906|Razorback Conglomerate|66190|5|Briefly described|p471 Fig.2,  p472|||Chert-rich conglomerate. Base composed of rounded to angular clasts of chert and subordinate quartzite (2-3mm) and becomes coarser higher in the section. Siliceous.||||||05-JUL-13
15906|Razorback Conglomerate|69850|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||Unit in Dundas Group.|||Interbedded, poorly-sorted, chert-rich conglomerate, pebbly sandstone and sandstone with lenses and interbeds of felsic volcanic detritus.|
15906|Razorback Conglomerate|69874|4|Described|p148-149, p163, p168|Boomerangian|Undillan|Dundas area. Contains the first felsic volcanic detritus recognised in this basin. Is of the same age as the Tyndall Group. [The text appears equivocal as to its parent unit. It is shown as part of the Lower Dundas Group on p149; is described as being "probably of Tyndall Group age" on p163; and on p168 "the Tyndall Group is considered to be represented by...Razorback Conglomerate..."].||||Overlies Hodge Slate. Underlies Lower Brewery Junction Formation.|Conglomerate with abundant chert clasts, as well as felsic volcanic detritus; unfossiliferous.|
15906|Razorback Conglomerate|70753|6|Mentioned|p183-184|Middle Cambrian|Middle Cambrian|||||Conformably overlies Hodge Slate. Is overlain conformably/gradationally by Brewery Junction Formation.||
73808|Read Lead Conglomerate|638|5|Briefly described|p88 Fig. 4.2|Middle Cambrian|Middle Cambrian|Of the Dundas Group. ||||||
81517|Red Heemskirk Granite|71100|5|Briefly described|p126-127,129-130,132,134|Famennian|Famennian|Weakly metaluminous to moderately peraluminous I-type granite. Also referred to as Heemskirk Red on p126. Of the Heemskirk Granite, red phase defined by consistent K-feldpsar (red K-spar) colour differences. Rb-Sr whole rock age of 357+\-7 Ma from Brooks and Compston, 1995. Recent SHRIMP zircon dating yields U-Pb age of 360+\-2 Ma (Black et al., 2005).|360+\-2 Ma||||Fine- to coarse-grained, equigranular, locally porphyritic. Quartz, K-feldspar, plagioclase, and minor biotite, trace zircon, monazite, titanite, magnetite/ilmenite, apatite, fluorite, hornblende and allanite.|
15943|Red Hill dolerite complex|41895|6|Mentioned|p25|||||||||
15950|Red Lead Conglomerate|40890|6|Mentioned|p53|||||||||
15950|Red Lead Conglomerate|41795|3|Fully described|p39, Fig. 13|Middle Cambrian|Middle Cambrian|||||||02-APR-07
15950|Red Lead Conglomerate|41814|6|Mentioned|Map legend|Cambrian||||||||
15950|Red Lead Conglomerate|43131|6|Mentioned|Fig.9,p582|||||||||
15950|Red Lead Conglomerate|43777|5|Briefly described|p2||Cambrian|||||||
15950|Red Lead Conglomerate|44135|5|Briefly described|p18|||In places underlain by Judith Formation. Lies with erosional contact on a succession of intercalated basaltic pillow lavas and volcanic breccias forming part of Serpentine Hill Complex. Contains ultramafic detritus from this source.||||||07-DEC-09
15950|Red Lead Conglomerate|63168|4|Described|p47, p66, p75 Fig. 3.10|Middle Cambrian|Middle Cambrian|Of the Dundas Group. Overlies Judith Formation; conformably underlies Hodge Formation. Series of poorly sorted, volcaniclastic, polymict conglomerate units of mass flow origin, interbedded with lenticular siltstone and sandstone horizons. ||||||
15950|Red Lead Conglomerate|63169|6|Mentioned|p179|||Described by Brown (1986) in Kapi Creek-Ring River area. Basal unit in Dundas Group. Passes conformably upwards into Hodge Slate. Detailed lithology is included.||||||
15950|Red Lead Conglomerate|63238|5|Briefly described|p12, p20 Fig. 3|Middle Cambrian|Middle Cambrian|Of the Lower Dundas Group.||||||
15950|Red Lead Conglomerate|63240|6|Mentioned|p4|||Formerly part of "lower Dundas Group" (lower section) - now redesignated as Western Volcano-Sedimentary Sequence.||||||
15950|Red Lead Conglomerate|64395|5|Briefly described|p174 Fig. 8.|||||||||07-FEB-11
15950|Red Lead Conglomerate|69850|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||Unit in Dundas Group.|||Poorly-sorted, volcaniclastic (in places mafic, in other places felsic) polymict conglomerate.|
15950|Red Lead Conglomerate|69874|4|Described|p122, p132, p148-149, p163|Middle Cambrian|Middle Cambrian|Dundas area. Described as "locally derived". Clasts of Serpentine Hill Ultramafic Complex basalt in Red Lead Conglomerate and blocks of conglomerate in upper lava flows, imply coeval relationship. Shown as Floran stage of Drumian of Series 3 of Middle Cambrian. Equivalent of the Western Volcano-Sedimentary Sequences.||Basal Dundas Group.||Overlies Judith Formation. Underlies Hodge Slate. Interdigitates with Serpentine Hill Ultramafic Complex. Faulted against Dundas Ultramafic Complex.|Mass flow conglomerate units containing clasts of serpentinite and chromite, quartzite, chert, jasper, carbonate and siltstone.|
15950|Red Lead Conglomerate|70753|6|Mentioned|p183-184|Middle Cambrian|Middle Cambrian|||||Overlies Judith Formation. Is overlain conformably by Hodge Slate.||
37156|Red Reef Cliff Siltstone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
37156|Red Reef Cliff Siltstone|69875|5|Briefly described|p258 Fig 5.13, p262|Emsian|Emsian|70m thick. Age inferred from Fig 5.13.||Spero Bay Group||Overlies Point Hibbs Limestone conformably. Underlies Whitehorses Beach Sandstone conformably.|Unfossiliferous redbed sequence of lithic sandstone and conglomerate arranged in fining-upward sequences.|
15966|Red Rock clastics|38260|6|Mentioned|p200|||||||||
79594|Red Rock member|69876|5|Briefly described|p352|||Renison Bell mine.||Crimson Creek Formation.|||Conglomerates, agglomerates, cherts, tuffs; minor shales and sandstones.|
37074|Redwater Granite|23718|6|Mentioned|p74|||||||||
37070|Redwater Granite""|23718|5|Briefly described|p74|||||||||
16003|Regency formation|41993|6|Mentioned|Fig.8 P14|||||||||
16018|Rekunian Series|30150|2|Defined|p93|Triassic|Permian|Permo-Triassic||||||
16018|Rekunian Series|38908|6|Mentioned|p6|||||||||
16018|Rekunian Series|39680|6|Mentioned|Map legend|Permian|Permian|||||||
16018|Rekunian Series|41696|6|Mentioned|Map legend|Permian||Tasmanian time period, not stratigraphic name.||||||
16018|Rekunian Series|44135|6|Mentioned|p43|||Of Clarke and Farmer (1976). Probably an obsolete name.||||||07-DEC-09
25439|Renison Bell Complex|31669|6|Mentioned|p72|||||||||
16023|Renison Bell Granite|37053|6|Mentioned|Table 14|||Isotopic data.||||||
16023|Renison Bell Granite|40070|6|Mentioned|p19|||||||||
16024|Renison Bell Member|22770|4|Described|Fig3p769|Neoproterozoic|Neoproterozoic|Of the Success Creek Group.||||||02-OCT-07
16024|Renison Bell Member|33218|5|Briefly described|p37|||||||||
16024|Renison Bell Member|64394|5|Briefly described|p98|||Comprises 3 subunits informally called RBM Lower (20-40m of massive fine-grained quarts sandstone); RBM Middle (laminated micaceous black shale + local thin siltstone/sandstone laminae) and RBM Upper, distinguished from RBM Middle by increasing carbonate.||||||10-NOV-08
16024|Renison Bell Member|69876|5|Briefly described|p352|||Renison Bell mine.||Success Creek Group.|||Siltstones, shales, sandstones, quartzites, dolomite pebble marker beds.|
16026|Renison Bell Shale|31832|6|Mentioned|Fig. 12|||||||||
16026|Renison Bell Shale|32409|5|Briefly described|p582|||||||||
16026|Renison Bell Shale|33839|6|Mentioned|p569|||||||||
16026|Renison Bell Shale|37053|5|Briefly described|p394|||||||||
16026|Renison Bell Shale|38261|6|Mentioned|p203|||||||||
16025|Renison Bell Shale""|41795|6|Mentioned|p23|||||||||
16025|Renison Bell Shale""|63168|6|Mentioned|p51|||Superseded by Renison Bell Formation. Considered to overlie Dolcoath Formation conformably. ||||||
16027|Renison Bell granites|37053|6|Mentioned|p420|||||||||
34491|Renison Dolomites|22770|6|Mentioned|Fig5 p770|||Not intended as a formal name? Compound term used to embrace all the dolomites of the Renison Mine region referred to as No. 1 Dolomite (within the Crimson Creek Formation) and  No. 2 Dolomite and No. 3 Dolomite within the Success Creek Group.||||||02-OCT-07
16028|Renison Formation|41795|6|Mentioned|p33|||||||||
16029|Renison Granite|24271|6|Mentioned|p1637|||||||||
16029|Renison Granite|24273|6|Mentioned|p1663|||||||||
16029|Renison Granite|24274|6|Mentioned|p1690|||||||||
16029|Renison Granite|42726|5|Briefly described|map legend|Late Devonian||Variation on Renison Bell Granite?||||||
16029|Renison Granite|60423|5|Briefly described|p381|Early Carboniferous|Late Devonian|Age: 355 +/- 4Ma (Brooks, 1966).||||||
16029|Renison Granite|61216|5|Briefly described|p19 Fig. 7|||Presented as Renison only in map of granites.||||||10-FEB-11
16029|Renison Granite|63540|5|Briefly described|Map legend||Devonian|Presented as compound name of  Renison/Pine Hill (granites). Of the Renison Suite. One of west Tasmanian granites.  I-type granite, felsic; strongly fractionated, reduced. Name implied from map legend.||||||26-SEP-07
16029|Renison Granite|69874|5|Briefly described|p127 Fig 4.26|Devonian|Devonian|Shown as (Pine Hill/Renison Granite) p127 Fig 4.26.|||||Quartz porphyry and massive quartz bodies.|
16029|Renison Granite|69876|4|Described|p304,306Tb 6.1, p307-308, p315, 317,318-|Carboniferous|Carboniferous|Single body Suite. I-type granite. Geochemistry. Equigranular and porphyritic varieties with K-feldspar and quartz phenocrysts. Crystal-fractionated. Multiple intrusive phases; cut by porphyritic, aplitic and microgranite dykes. See also p300.|~349-341 Ma (Rb-Sr).|Renison Suite|||I-type. Pale grey-white, fine-coarse grained, biotite adamellite/alkali-feldspar granite: quartz, perthitic K-feldspar(white), plagioclase, biotite, magnetite; accessory apatite, zircon, ilmenite, monazite, tourmaline, fluorite, topaz.|16-JAN-17
16029|Renison Granite|71730|5|Briefly described|p7, p32, p34, p36, p39,|||Western Tasmania. Moderate mean heat generation. [Formal name not originally intended] Author combines Renison and Pine Hill Granite on p39 into ""Renison-Pine Hill Granite"". See also  p58, p60.|||||I-type granite variably and locally intensley altered.|
42331|Renison granite|24273|5|Briefly described|p1663|Early Carboniferous|Late Devonian|Age: 355+/-4 Ma.||||||
16044|Reservoir andesite|35844|4|Described|p43|||Petrology.||||||
16044|Reservoir andesite|64395|5|Briefly described|p172|||Informal name. Hornblende-phyric andesite occurring mainly as intrusives within the upper part of southern Central Volcanic Complex; together with Anthony Road and Crown Hill andesites these form Suite 2 of Mount Read Volcanics.||||||07-FEB-11
74580|Rhyndaston Formation|63868|6|Mentioned|p17|||Term 'formation' is used in grouping together several named units and is therefore probably an informal name.||||||07-FEB-11
74582|Rhyndaston Sandstone|63868|6|Mentioned|p17|||Of David (1932).||||||07-FEB-11
83425|Riana Dolerite|69842|6|Mentioned|p6|Cambrian|Cambrian|Riana map; previously considered Ordovician.||||Correlated with (Cambrian) Lobster Creek Intrusives.||
83426|Rinadeena Shale|69842|6|Mentioned|p7|Ordovician|Ordovician|Teepookana map; a large area added in the Open Creek area. Age inferred from Ola map symbol.||||||07-JUL-22
79054|Rinadeena Shale""|69859|5|Briefly described|Map legend|Ordovician|Ordovician|||Unit in Gordon Group.|||Siltstone.|
79054|Rinadeena Shale""|73320|6|Mentioned|Map legend|Ordovician|Ordovician|Western Tasmania. Map unit includes Arndell Sandstone, 'Rinadeena Shale' and correlates; description of mainly siltstone and fine-grained sandstone.||||||10-MAY-22
16113|Risdon Formation|24549|5|Briefly described|p7|||Max Thickness: 30ft.||||||
16113|Risdon Formation|41895|6|Mentioned|p83|||||||||
16113|Risdon Formation|43021|5|Briefly described|Fig.2,p462|||Variation on Risdon Sandstone?||||||
16113|Risdon Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Permian|Late Permian|Informal - see Risdon Sandstone. Overlain by Abels Bay Formation; overlies Minnie Point Formation and Malbina Formation.  See also p304 Fig. 8.7.||||||07-FEB-11
16113|Risdon Formation|67501|6|Mentioned|p7|||See reference to Risdon Sandstone (p18, Fig.8 p17).||Parmeener Supergroup|||Coarse-grained sandstone.|
75746|Risdon Sandstone member|66174|14|Not recorded|?|||||||||
16115|Risdon Siltstone|30153|6|Mentioned|Fig.45|||||||||
27551|Risdon sandstone|31758|6|Mentioned|Map legend|Permian|Permian|Permian. Ferntree Group.||||||
74128|Risdon sandstones|63820|5|Briefly described|Map legend|Permian|Permian|||||||
78547|Rocky Cape Dyke Swarm|67502|6|Mentioned|p41, p102, p103|||Informal and invalid term replaced by Tayatea Dyke Swarm.||||||
78547|Rocky Cape Dyke Swarm|73313|5|Briefly described|Map legend|Cryogenian|Cryogenian||||||Tholeiitic dolerite dykes.|
78547|Rocky Cape Dyke Swarm|73320|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||||Tholeiitic dolerite.|
25448|Rocky Cape Formation|39475|6|Mentioned|p404|||||||||
16233|Rocky Cape Group quartzites|35288|6|Mentioned|p12|||||||||
81292|Rocky Cape Group, lower-middle|69553|5|Briefly described|p50,59,63,64|Proterozoic|Proterozoic|Geological province: Western Tasmania Terrane. NW Tasmania. Approximately 9km thick and deposited after c. 1450 Ma. Dominated by detrital zircon populations between 1600 and 1900 Ma. Likely has a shared provenance with the higher-grade metasediments of the Surprise Bay and Fraser formations.|||Includes Pedder River Siltstone, Lagoon River Quartzite, Balfour Subgroup, Detention Subgroup.|||
16234|Rocky Cape Quartzite|30877|6|Mentioned|p7|||||||||
16235|Rocky Cape formation|38638|6|Mentioned|p1910|||||||||
74393|Rocky Cape group|63170|6|Mentioned|p192|Precambrian|Precambrian|Forms many of the clasts making up Duncan Conglomerate of the Dial Group.||||||07-FEB-11
16242|Rocky Gape formation|38638|6|Mentioned|p1902|||Misspelling of Rocky Cape?||||||
16258|Roland Conglomerate Formation|41954|6|Mentioned|Table 1 P12|||||||||
16259|Roland Conglomerate""|42204|6|Mentioned|p233|||||||||
16259|Roland Conglomerate""|44135|6|Mentioned|p27|||Informal - see Roland Conglomerate. Corresponds to basal conglomerate of the Moina Sandstone, plus some elements of underlying units.||||||07-DEC-09
74072|Roland conglomerate|61395|6|Mentioned|p16|||Informal name. In northern Tasmania. Unconformity separates this unit from the younger Moina Sandstone.||||||07-FEB-11
16305|Rooks River granite|36374|3|Fully described|p58|||||||||
16325|Rosbery Group|30278|6|Mentioned|p186|||Refers to Loftus Hills et al(1967)and Braithwaite(1972)||||||
16332|Roseberg Group|31174|6|Mentioned|p170|||Refers to Taylor (1954)||||||
16333|Rosebery "Group"|39892|6|Mentioned|p20|||||||||
16333|Rosebery "Group"|42387|6|Mentioned|p267|||||||||
16334|Rosebery Group|29914|5|Briefly described|Fig.1|||||||||
16334|Rosebery Group|29930|6|Mentioned|p1087|||||||||
16334|Rosebery Group|30032|6|Mentioned|p621|||||||||
16334|Rosebery Group|30281|6|Mentioned|p7|||Refers Taylor(1954)||||||
16334|Rosebery Group|33218|5|Briefly described|p7|||||||||
16334|Rosebery Group|33839|5|Briefly described|p570|||||||||
16334|Rosebery Group|37044|6|Mentioned|Fig.8|||||||||
16334|Rosebery Group|37045|6|Mentioned|p221|||||||||
16334|Rosebery Group|37049|6|Mentioned|p306|||||||||
16334|Rosebery Group|40070|4|Described|p9|||||||||
16334|Rosebery Group|40736|6|Mentioned|Fig.4|||||||||
16334|Rosebery Group|40967|6|Mentioned|p89|||||||||
16334|Rosebery Group|40978|6|Mentioned|p320|||||||||
16334|Rosebery Group|41148|6|Mentioned|Fig.7|||||||||
16334|Rosebery Group|41795|6|Mentioned|Fig.3|Cambrian||||||||
16334|Rosebery Group|41814|6|Mentioned|Map legend|Cambrian||||||||
16334|Rosebery Group|43054|6|Mentioned|p30|||||||||
16334|Rosebery Group|61412|6|Mentioned|p45.|||Fig.34 on p45 suggests Mount Charter Group includes Rosebery Group.||||||
16334|Rosebery Group|69850|5|Briefly described|Map legend|Cambrian|Cambrian|Nine separately-mapped units in the Colebrook Hill - Mount Dundas area are named collectively as a correlate of Rosebery Group. These units include correlates of Stitt Quartzite, Westcott Argillite and Salisbury Conglomerate.|||Includes Stitt Quartzite, Westcott Argillite and Salisbury Conglomerate.|||
16334|Rosebery Group|69857|5|Briefly described|Map legend|||||||||
16334|Rosebery Group|69874|5|Briefly described|p122, p139, p213, p229|Late Cambrian|Middle Cambrian|Taylor (1954), Campana and King (1963). A correlate of the Owen Group [and thus presumably redundant].||||Correlate of Owen Group.|Volcaniclastic and siliceous units.|
28976|Rosebery Group""|638|6|Mentioned|p99|||Of Brathwaite (1974); Green et al (1981). Superseded the original "Rosebery Series" and is now part of the Dundas Group. A volcano-sedimentary sequence abutting the Central Volcanic Complex at Rosebery. ||||||
28976|Rosebery Group""|31174|6|Mentioned|Fig. 37|||||||||
28976|Rosebery Group""|39892|6|Mentioned|p20|||||||||
28976|Rosebery Group""|40890|6|Mentioned|Fig.3|||||||||
28976|Rosebery Group""|41795|6|Mentioned|p37|||||||||
28976|Rosebery Group""|63238|5|Briefly described|p10, p22|||Seq. to west of Rosebery Fault now reassigned to Owen Gp due to Cambrian fossil evidence, incl:Stitt Quartzite+correlates, Westcott Argillite and Salisbury Conglom. Original E. part of group (in part "Primrose Pyroclastics") now correlated with Tyndall Gp||||||
28976|Rosebery Group""|63240|6|Mentioned|p3|||Parts now designated as marine Owen Group.||||||
28976|Rosebery Group""|69859|5|Briefly described|Map legend|Cambrian|Cambrian|Unclear from the legend as to whether this unit is a Formation in Denison or Owen Group.||Unit in Wurawina Supergroup.|||Marine sandstone-siltstone-conglomerate sequences, typically turbiditic, quartz-rich to polymict; Furongian fossils in places.|
28976|Rosebery Group""|73313|6|Mentioned|Map legend|Furongian|Furongian|Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, siliciclastic to polymict, Furongian fossils in places.||Owen Group||||
28976|Rosebery Group""|73320|6|Mentioned|Map legend|Furongian|Furongian|Western Tasmania. Map unit includes Newton Creek Sandstone, Middle Owen Sandstone, upper Dundas Group, much of 'Rosebery Group'; description of marine sandstone-siltstone-conglomerate sequences, typically turbiditic, quartz-rich to polymict; Furongian fossils in places. Grouped in either Owen Group, Dension Group and correlates.||||||10-MAY-22
16335|Rosebery Mine schist|39892|6|Mentioned|p20|||Variation of Rosebery Schist?||||||
16336|Rosebery Schist|39892|6|Mentioned|p16|||Table 2||||||
16337|Rosebery Series""|638|6|Mentioned|p99|||Of Finucane (1932); Campana and King (1963); Loftus-Hills eta al (1967). Original name for a volcano-sedimentary sequence abutting the Central Volcanic Complex at Rosebery. Superseded by "Rosebery Group". ||||||
16337|Rosebery Series""|41795|6|Mentioned|p49|||||||||
16338|Rosebery Slates|33839|6|Mentioned|Fig.3|||||||||
16339|Rosebery group|33218|6|Mentioned|Fig.3|||||||||
73295|Rosebery shale|63238|5|Briefly described|p19 Fig. 2|||Informal - see "Rosebery Group". ||||||
16360|Ross Formation|24549|4|Described|p5|Triassic|Triassic|Max. Thickness: ~650ft. Predominantly medium-grained quartz sandstone.||||||07-FEB-08
16360|Ross Formation|30455|6|Mentioned|p12|||Lower Triassic age||||||
16360|Ross Formation|30458|6|Mentioned|p14|||Triassic age||||||
16360|Ross Formation|30460|6|Mentioned|p7|||See also P8,12,26. Lower Triassic age||||||
16360|Ross Formation|30466|6|Mentioned|p8|||Triassic age||||||
16360|Ross Formation|32627|5|Briefly described|p32|Triassic|Triassic|Thickness: 198m. Impure, medium-grained quartz sandstone.||||||07-FEB-08
16360|Ross Formation|35873|6|Mentioned|p93|||||||||
16360|Ross Formation|35901|6|Mentioned|p11|||||||||
16360|Ross Formation|36899|6|Mentioned|p1092|||||||||
16360|Ross Formation|41699|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
16360|Ross Formation|41910|5|Briefly described|p127|||||||||
16360|Ross Formation|42244|4|Described|p9, p26|||Type section is not at Ross but 50km away at Poatina. Ross Formation superseded by Ross Sandstone - or vice versa? This is unclear.||||||14-AUG-08
16360|Ross Formation|43072|6|Mentioned|p56|||||||||
16360|Ross Formation|43923|6|Mentioned|p12||Early Triassic|||||||
16360|Ross Formation|63172|5|Briefly described|p316|||Overlain by Cluan Formation. Thickness: 200m.||||||07-FEB-11
16360|Ross Formation|63868|6|Mentioned|p17|||Term 'formation' used in grouping together several named units and is therefore probably an informal name.||||||07-FEB-11
16360|Ross Formation|67501|6|Mentioned|p7|Early Triassic|Early Triassic|||||Corresponds to the upper part of Upper Parmeener Supergroup.||
16360|Ross Formation|69877|5|Briefly described|p378-380|Early Triassic|Early Triassic|Deposition by low-sinuosity rivers flowing ESE. Similar flora to Narrabeen Group (Sydney Basin).||Unit in Upper Parmeener Supergroup.||Equivalent to (lower) Cluan Formation, Mountain Lodge Member, Knocklofty Formation, Ossa Formation and (part) Gould Conglomerate.|Well-sorted, glistening quartz sandstone in fining-upward cycles, often with basal mud-pellet conglomerate or quartz granules; cycles are massive or tabular, cross-bedded or planar-laminated, scour fills.|
16363|Ross Sandstone Formation|30819|6|Mentioned|p108|||||||||
16363|Ross Sandstone Formation|71540|6|Mentioned|p288 Fig.1|||Caveside area.||||||
40010|Ross Sandstone and Shale|24548|6|Mentioned|Reverse side of Map 4687|Triassic|Triassic|Informal name||||||
16364|Ross Sandstone""|42244|6|Mentioned|p26|||Informal name. One of the names used for the sandstone at Ross; others include Ross Series, Ross Formation and Ross Sandstone.||||||12-AUG-08
74130|Ross Sandstones|63820|5|Briefly described|Map legend|Triassic|Triassic|||||||
16366|Ross sandstones|39023|6|Mentioned|p402|||||||||
16394|Rowallan Till|30524|6|Mentioned|Table 2|||Lithostratigraphical relationships. Pleistocene||||||
16436|Rum Island Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
16457|Rupert Beds|34188|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
70298|Russells Road suite|61723|6|Mentioned|p817|||Informal name. Includes the Upper Blessington Granodiorite, Hogarth Road Granite and Tombstone Creek Granite.||||||
16524|Saint Clair Formation (TAS)|30524|6|Mentioned|Table 2|||Lithostratigraphical relationships. Pleistocene||||||
16524|Saint Clair Formation (TAS)|40439|6|Mentioned|p374|||||||||
16534|Saint Helens granodiorite|33354|5|Briefly described|p180|||Detailed mapping of dykes.||||||
16534|Saint Helens granodiorite|37797|6|Mentioned|p152|||||||||
78601|Saint Mary's Porphyry|65716|5|Briefly described|p33|||St in text. Also called Saint Mary's porphyrite. ~385 Ma.||||||
16547|Saint Mary's Volcanics|42726|5|Briefly described|map legend|||Variation/misspelling on Saint Marys Porphyrite.||||||
75747|Saint Marys Basal Stage|66174|14|Not recorded|?|||||||||
73644|Saint Marys Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Scamander Tier Suite,  Blue Tier Batholith. I-type granite, mafic; unfractionated, reduced. Name implied from map legend.||||||
16549|Saint Marys Porphyrite|22627|6|Mentioned|p132, fig8p137|||||||||
16549|Saint Marys Porphyrite|22768|6|Mentioned|Fig16.5p164|||Saint is St in text.||||||18-SEP-07
16549|Saint Marys Porphyrite|22857|6|Mentioned|p164 Fig. 16.5|||Age: ~388+/-1Ma. Saint is St. in text.||||||
16549|Saint Marys Porphyrite|23467|5|Briefly described|p282|Early Devonian|Early Devonian|Age: 388+/-1Ma.||||||18-SEP-07
16549|Saint Marys Porphyrite|23850|5|Briefly described|p791|Early Devonian|Early Devonian|Saint is St. in text.||||||
16549|Saint Marys Porphyrite|33732|6|Mentioned|p109|||||||||
16549|Saint Marys Porphyrite|37501|6|Mentioned|p405|||||||||
16549|Saint Marys Porphyrite|40310|6|Mentioned|p248|||||||||
16549|Saint Marys Porphyrite|40660|4|Described|p203|||||||||
16549|Saint Marys Porphyrite|40760|5|Briefly described|p178|||||||||
16549|Saint Marys Porphyrite|41691|6|Mentioned|Map legend|Devonian||||||||
16549|Saint Marys Porphyrite|41855|3|Fully described|p44|||Also Described, p13.||||||18-SEP-07
16549|Saint Marys Porphyrite|42878|6|Mentioned|p169|||actually spelt St Marys Porphyrite||||||
16549|Saint Marys Porphyrite|43584|5|Briefly described|p56|Devonian||||||||
16549|Saint Marys Porphyrite|44135|5|Briefly described|p42|Early Devonian|Early Devonian|Age: 388+/-1Ma. Dacitic ash-flow (extrusive). Saint is St in text.||||||07-DEC-09
16549|Saint Marys Porphyrite|48894|6|Mentioned|p79|||Age of emplacement: 374 m.y.||||||13-MAY-22
16549|Saint Marys Porphyrite|73369|5|Briefly described|p302, p328, p329|||See also discussion p301-302. Two samples dated. K-Ar age 375 m.y.||||||
16548|Saint Marys Porphyrite volcanics|40310|6|Mentioned|p252|||||||||
16550|Saint Marys Porphyry|41855|6|Mentioned|p67|||||||||
16550|Saint Marys Porphyry|43084|6|Mentioned|p37|||Saint is St in text.||||||03-OCT-07
16550|Saint Marys Porphyry|43547|14|Not recorded|p160|||Age: 370 million years.||||||03-OCT-07
16550|Saint Marys Porphyry|66174|14|Not recorded|?|||||||||
16550|Saint Marys Porphyry|69856|5|Briefly described|Map legend|Devonian|Devonian|||||Unconformably overlies Mathinna Supergroup.|Dominantly felsic pyroclastic rocks: volcanic equivalent of I-type granodiorite.|
16550|Saint Marys Porphyry|71100|5|Briefly described|p126,136|||Partly extrusive equivalent of I-type granodiorite (e.g. Blue Tier and Scottsdale Batholiths). Formed by slab rollback of the W-dipping subduction zone east of Australian Gondwanan margin until c. 390 Ma.||||||
28984|Saint Marys granite|31577|6|Mentioned|p80|||370 m.y.||||||
16552|Saint Marys porphyrite|39927|4|Described|p305|||||||||
16552|Saint Marys porphyrite|40310|6|Mentioned|p252|||||||||
16563|Salisbury Conglomerate|37045|6|Mentioned|p221|||||||||
16563|Salisbury Conglomerate|41795|6|Mentioned|p41|||||||||
16563|Salisbury Conglomerate|63238|5|Briefly described|p10, p22|||Formerly of the ""Rosebery Group" - now reassigned to Owen Group based on Cambrian fossil evidence. ||||||
16563|Salisbury Conglomerate|69850|5|Briefly described|Map legend|Cambrian|Cambrian|Has an un-named correlate consisting of poorly sorted, massive to bedded, polymict, calcareous conglomerate, in the Colebrook Hill - Mount Dundas area.||Unit in Rosebery Group.||||
16563|Salisbury Conglomerate|69874|5|Briefly described|p122|Late Cambrian|Late Cambrian||||||Polymict conglomerate with detrital fuchsite.|
73302|Salisbury Conglomerate""|63238|5|Briefly described|p20 Fig. 3|Late Cambrian|Late Cambrian|Of the "Rosebery Group". ||||||
73276|Salisbury fuchsitic conglomerate|63240|5|Briefly described|p4|||Redesignated from "Rosebery Group" to marine Owen Group from fossil evidence and lithology, together with Stitt Quartzite, Munro Creek Slate and Quartzite, Westcott dolomitic beds, and Natone Volcanics.||||||10-DEC-07
78554|Salmon River Dolomitic Breccia|67502|6|Mentioned|p55|||Superseded; ?equivalent to the Julius River Member; rarely used, not formally defined; of Matthews (1961) who considered it part of the 'Trowutta Group' (roughly synonymous with the Kanunnah Subgroup); may have confused it with another diamictite unit (Croles Hill Diamictite).||Trowutta Group of Matthews (1961b),||||16-DEC-13
16582|Sanctuary Bay Sandstone|33732|4|Described|p109|||||||||
16582|Sanctuary Bay Sandstone|41317|6|Mentioned|p172|||||||||
16582|Sanctuary Bay Sandstone|43547|14|Not recorded|Table p158-60||Eifelian|Part of Spero Bay Group||||||
24624|Sassafras Creek Member|42478|5|Briefly described|Fig.21 P19|||Variation of Sassafras Creek Formation||||||03-OCT-07
24624|Sassafras Creek Member|50091|5|Briefly described|p413 Tb.1|Late Ordovician|Late Ordovician|This name probably intended by Sass Ck Mem in Table 1?  Occurrence of Panderodus nogamii (conodonts) - in the Mole Creek area.||||||
16633|Sassafras Formation|13995|5|Briefly described|p70|Ordovician|Ordovician|Mole Creek.||Chudleigh Subgroup.||||
16633|Sassafras Formation|42416|5|Briefly described|p192|||Variation of Sassafras Creek Formation?||||||
16633|Sassafras Formation|43668|6|Mentioned|Fig.8,p12||Gisbornian|||||||
73809|Sassy Creek Argillites|638|5|Briefly described|p117|||Sequence of interbedded phyllitic black shales, greywackes and dolomite. Passes westward into Mainwaring Group. ||||||
16639|Savage River Iron ore deposits|30763|6|Mentioned|p34|||||||||
16640|Savage River amphibolite|39892|6|Mentioned|p30|||||||||
16641|Savage dolomites|38638|6|Mentioned|p1901|||||||||
29256|Scamander Quartzite and Slate|40660|6|Mentioned|p215|||||||||
29256|Scamander Quartzite and Slate|41855|6|Mentioned|p10|||||||||
29256|Scamander Quartzite and Slate|63170|6|Mentioned|p234|||Part of the former 'arenite-lutite association' of Banks (1962e) together with Mathinna Slate and Quartzite and Fingal beds.||||||07-FEB-11
31326|Scamander Sandstone|43533|14|Not recorded|Tb p152,158,160-1|||Part of Mathinna Beds (Skalian)||||||
31326|Scamander Sandstone|43547|14|Not recorded|Tb p152,158,160-1|||Part of Mathinna Beds (Skalian)||||||
31325|Scamander Siltstone|43533|14|Not recorded|Tb p152,158-160|||(Skalian)||||||
31325|Scamander Siltstone|43547|14|Not recorded|Table 152,158-60|||(Skalian)||||||
75740|Scamander Slate and Quartzite|66172|4|Described|p25, 23|Devonian|Silurian|Unit description given. Correlated with Mathinna Group. Intruded by Saint Marys Porphyrite.||||||09-SEP-10
75740|Scamander Slate and Quartzite|66174|14|Not recorded|23|||||||||09-SEP-10
75740|Scamander Slate and Quartzite|66175|6|Mentioned|183|||||||||
78560|Scamander Tier Dyke|67503|4|Described|p9 and throughout.|Givetian|Givetian|Associated (geochemical and mineralogical = comagmatic) with St Marys Porphyrite. Intruded along major faults, probable F1, post-dates major tectonic structures in the country rocks. Steeply dipping contacts, narrow chilled margin, contact metamorphism. Outcrop displaced by Orieco Fault.|388 +/- 1 Ma Rb-Sr and K-Ar (Turner et al. 1986).|||Intrudes the sediments of the Mathinna Supergroup. Feeder to the St Marys Porphyrite. Related to the Catos Creek Dyke.|Porphyritic microgranodiorite.|27-MAY-14
16655|Scamander Tier Granite|42726|5|Briefly described|map legend|Middle Devonian||Variation on Scamander Tier Granodiorite.||||||
16655|Scamander Tier Granite|61216|5|Briefly described|p20 Fig. 7a|||Presented as Scamander Tier only in map of granites. I-type granite.||||||10-FEB-11
16655|Scamander Tier Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Scamander Tier Suite,  Blue Tier Batholith. I-type granite, mafic; unfractionated, reduced. Name implied from map legend.||||||
16655|Scamander Tier Granite|66575|6|Mentioned|p936 Fig2|||Mafic, unfractionated, I-type hornblende-biotite granodiorite.||||||
16655|Scamander Tier Granite|69876|5|Briefly described|p304, p308, p313|Middle Devonian|Middle Devonian|Blue Tier Batholith. Geochemistry, Sr ratios.|c.397-385 Ma (Rb-Sr).|Scamander Tier Suite|||I-type.|
16656|Scamander Tier Granodiorite Porphyry|35827|6|Mentioned|p29|||Refers Cocker (1971).||||||03-OCT-07
16658|Scamander Tier granodiorite|37797|6|Mentioned|p139|||||||||
16658|Scamander Tier granodiorite|39927|6|Mentioned|p305|||||||||
16658|Scamander Tier granodiorite|40310|6|Mentioned|p249|||See also P255||||||
16659|Scamander Tier microgranodiorite|40660|6|Mentioned|p215|||||||||
16660|Scamander granodiorite|37797|6|Mentioned|p141|||||||||
16672|Schnells Ridge quartzite|42227|6|Mentioned|p28|||Informal name - probably not intended as a stratigraphic name.  Refers to quartzite at Schnells Ridge.||||||16-JUN-09
27894|Scotchfire Group|30616|4|Described|p192|||See also p191. Equivalent? Joyce Group.||||||03-OCT-07
27894|Scotchfire Group|45087|5|Briefly described|p225|||Chemical analyses.||||||03-OCT-07
73115|Scotchfire Metamorphics|44135|5|Briefly described|p33|||Conformably overlain by Jane Dolomite. Comprise lower greenschist facies, consisting of schistose fine-grained sandstone or siltstone and dark grey mudstone.||||||07-DEC-09
40011|Scott-Quartz Keratophyre|24548|5|Briefly described|Maps 4687 and 46-88|Cambrian|Cambrian|Probably misspelt? See also Scott Quartz Keratophyre. See also Deloraine Map 46-88||||||
16689|Scottsdale Granite|34316|5|Briefly described|p55|Devonian|Devonian|Granodiorite. Age: 370+/-10Ma. Intruded Mathinna Beds.||||||06-FEB-08
16689|Scottsdale Granite|61216|6|Mentioned|Fig. 12 p34-35|Devonian|Devonian|||||||10-FEB-11
16690|Scottsdale granite|31577|6|Mentioned|p80|||370 m.y.||||||
33456|Sea Elephant Adamellite|44105|4|Described|p257|||Of the Grassy Suite.||||||24-MAY-07
33456|Sea Elephant Adamellite|44135|5|Briefly described|p6|Early Carboniferous|Early Carboniferous|Located in the north of King Island. Considered to be a fractionated equivalent of Grassy Granodiorite and Bold Head Adamellite, and more felsic than these intrusives.||||||07-DEC-09
33456|Sea Elephant Adamellite|61216|5|Briefly described|p30|||Small body in eastern King Island. Similar to Grassy adamellite but more felsic and contains less amphibole and sphene; granodiorite is also present altho' predominantly it is of adamellite.||||||10-FEB-11
33456|Sea Elephant Adamellite|63674|5|Briefly described|p9|Devonian|Devonian|Classified as I-type monzogranite-granodiorite. Fractionated equivalent of Grassy and Bold Head Granodiorites. Intrudes Proterozoic sedimentary rocks (Grassy Group) of eastern King Island.||||||
33456|Sea Elephant Adamellite|65644|5|Briefly described|p6|Devonian|Devonian|Intrudes Proterozoic sediments on King Island. I-Type. Fractionated equivalent of the Grassy and Bold head plutons (more felsic).|||||Adamellite-granodiorite with minor amphibole and sphene.|27-MAR-12
16767|Serpentine Hill Complex|30281|4|Described|p7|||||||||
16767|Serpentine Hill Complex|31174|5|Briefly described|p172|||||||||
16767|Serpentine Hill Complex|32941|4|Described|p91|||See also pp92-106. Petrology.||||||04-OCT-07
16767|Serpentine Hill Complex|33218|6|Mentioned|Fig.19|||||||||
16767|Serpentine Hill Complex|33839|5|Briefly described|p570|||||||||
16767|Serpentine Hill Complex|35153|6|Mentioned|p183|||||||||
16767|Serpentine Hill Complex|37053|5|Briefly described|p397|||See also Fig.1.||||||
16767|Serpentine Hill Complex|40070|6|Mentioned|p10|||||||||
16767|Serpentine Hill Complex|40760|5|Briefly described|p167|||||||||
16767|Serpentine Hill Complex|41562|6|Mentioned|Fig.2|||||||||
16767|Serpentine Hill Complex|43191|6|Mentioned|p46|||||||||
16767|Serpentine Hill Complex|61412|5|Briefly described|p44, p46.|||Serpentinised ultramafics, gabbros and basalts thrust over ?early Cambrian Crimson Creek Formation. There are hornblende mylonites at the base of (westward-directed) thrust sheets, considered early Middle Cambrian in age.||||||16-MAY-17
16767|Serpentine Hill Complex|63168|6|Mentioned|p66, p69|||Discusses interpretations of various geologists.||||||
16767|Serpentine Hill Complex|63169|5|Briefly described|p158|||Informal name. Dominated by layered pyroxenite and dunite intruded by two-pyroxene gabbro. Geological Province: Dundas Trough.||||||26-OCT-07
16767|Serpentine Hill Complex|66190|6|Mentioned|p469, p472 Fig.3|||Low-Ti basalts. Overlain by the Dundas Group.||||||
16767|Serpentine Hill Complex|70753|5|Briefly described|p183|||||||Is overlain unconformably by Hodge Slate.|Includes basalts.|
16769|Serpentine Hill Ultramafic-Mafic Complex|41795|6|Mentioned|Fig.45|||||||||
16769|Serpentine Hill Ultramafic-Mafic Complex|69876|5|Briefly described|p357|Cambrian|Cambrian|At Black Hill, near Dundas, interfingering with Dundas Group sediments suggests possibly coeval with Cambrian Series 3 age sedimentation. Hornfelsed by Heemskirk Granite.|||Includes Viking and North Avebury intrusives.|Intrudes Dundas Group.|Low-titanium tholeiite lavas.|
16770|Serpentine Hill complex|37044|6|Mentioned|p195|||||||||
16770|Serpentine Hill complex|37053|6|Mentioned|p394|||||||||
16770|Serpentine Hill complex|41594|6|Mentioned|p27|||||||||
16770|Serpentine Hill complex|44135|6|Mentioned|p16|||Informal name. Contains asbestos.||||||07-DEC-09
16770|Serpentine Hill complex|63169|6|Mentioned|p160|||Informal - see Serpentine Hill Complex. G33Its basalts are overlain by Dundas Group basal sediments.||||||
16771|Serpentine Hill ultramafic complex|33218|6|Mentioned|p37|||||||||
16772|Serpentine Ridge Complex|41594|6|Mentioned|p59|||||||||
16776|Settlers Metamorphosed Greywacke|30889|6|Mentioned|p36|||||||||
16776|Settlers Metamorphosed Greywacke|73369|5|Briefly described|p320, p321, p332|||K-Ar biotite dates of 470 m.y. and 490 m.y. Probably metamorphic ages. Rocks considered to be Cambrian.||||||
35841|Settlers metamorphosed greywacke|23326|6|Mentioned|974|||Informal name - originally described by Green (1959). Now included in Settlers Schist.||||||18-APR-07
35841|Settlers metamorphosed greywacke|69874|5|Briefly described|p106|||Green (1959). Included in Settlers Schist. Absence of relict sedimentary features makes the term inappropriate; Reed et al. (2001) argue it is a metagranite.||||||
81725|Settlers metamorphosed greywackes|12179|6|Mentioned|p974|||Nomenclature of Green (1959). Superseded; see Settlers Schist.||||||
16780|Severn Slate""|41795|6|Mentioned|p39|||||||||
16850|Shoemaker Beds|13995|5|Briefly described|p85|||Burrett et al. (1983). Gisbornian-early Eastonian. Contains upper slope, pelagic and deep-water trilobite taxa (listed).||||||
16850|Shoemaker Beds|41080|6|Mentioned|p158|||||||||
16850|Shoemaker Beds|69875|5|Briefly described|p254|Eastonian|Gisbornian|Surprise Bay. 200m thick. Blind and large-eyed trilobites indicate deep-water and probably continental slope environment below 200m depth. Upper part is paler with bryozoans and brachiopods, probably reflecting shallowing of paleoenvironment. Graptolites and conodonts affinities discussed.||||Correlates with Benjamin Limestone.|Thinly interbedded dark grey micrite and shale, and minor carbonate turbidites.|
16872|Sideling basalt|31520|5|Briefly described|p27|||Magnetic anomalies.||||||
74070|Sidling Formation|61395|5|Briefly described|p3 Fig. 1.2, p20|Early Devonian|Early Devonian|Of the Mathinna Group. Turbidites. Overlies the Bellingham Formation. See also p4 Fig. 1.3.||||||07-FEB-11
34172|Sidling Sandstone|22627|6|Mentioned|p132|Ordovician|Ordovician|||||||
34172|Sidling Sandstone|23850|5|Briefly described|p790 Fig. 5|Devonian|Devonian|Of the Panama Group. Overlies the Bellingham Formation. See also the informal Sidling sandstone.||||||26-APR-06
34172|Sidling Sandstone|24220|5|Briefly described|p882 Fig. 3|||See also Sidling sandstone. Of the Panama Group. Geological Province: Tabberabberan Orogeny.||||||19-FEB-08
34172|Sidling Sandstone|44135|5|Briefly described|p41|Early Devonian|Early Devonian|Of the Mathinna Group. Thickness: ~2km. Of  feldspatholithic composition at top of the group, grading out of the sublithic Bellingham Formation below. Contains Early Devonian plant remains; graptolites and shelly fragments of Pragian age.||||||07-DEC-09
34172|Sidling Sandstone|61216|5|Briefly described|p5, p6 Fig. 1|||Of Mathinna Supergroup. Overlies Bellingham Formation.||||||10-FEB-11
34172|Sidling Sandstone|63635|5|Briefly described|p10 Fig. 4|||See also the frequently used name but informally presented Sidling sandstone.||||||
34172|Sidling Sandstone|63675|5|Briefly described|p17|Early Devonian|Late Silurian|2 km of feldspathic turbidites. Unit in Mathinna Group; overlies Bellingham Formation. Contains Late Silurian graptolites and Early Devonian shelly fossils. ||||||
34172|Sidling Sandstone|65646|6|Mentioned|p4 Fig.1, p5.|Early Devonian|Early Devonian|Unit in Mathinna Group. Overlies Bellingham Formation. [misspelling of Sideling Sandstone]||||||08-FEB-16
34172|Sidling Sandstone|67655|4|Described|p17|Early Devonian|Late Silurian|Thickness: about 2 km. Contains Late Silurian graptolites (Rickards et al., 1993) and Early Devonian shelly fossils (Rickards and Banks, 1979).||Mathinna Supergroup||Overlies Bellingham Formation.|Feldspathic turbidites.|08-FEB-16
34172|Sidling Sandstone|69876|5|Briefly described|p278|||Eastern Tasmanian Terrane.||Panama Group.||Overlies Bellingham Formation.||
36811|Sidling sandstone|23850|5|Briefly described|p786||Late Silurian|Informal name. Of Panama Group. Overlies the Bellingham Formation.||||||24-SEP-15
36811|Sidling sandstone|24220|5|Briefly described|p880|Devonian|Cambrian|Of the Panama Group.   Originally included in the Mathinna Group.  Informally defined name.  See also Sidling Sandstone.||||||19-FEB-08
36811|Sidling sandstone|63635|5|Briefly described|p9, p22, p23|Early Devonian|Late Silurian|Informal - see Sidling Sandstone. Of the Panama Group (Mathinna Supergroup). Turbidite facies overlying the Bellingham Formation.||||||15-NOV-10
36811|Sidling sandstone|67493|5|Briefly described|p6 Fig.1b, p7, p9, p10 Fig.3, p20, p74 |Early Devonian|Early Devonian|Powell et al. (1993). Informal, and mis-spelling of the topographic feature Sideling Range. Formalised and replaced by the Sideling Sandstone. Contains Early Devonian plant fossils. Overlies Bellingham Formation.||Panama Group||Overlying the superseded Bellingham Formation.||
16873|Sidling sandstone""|42878|6|Mentioned|Fig.1, P170|||Assume intended as informal name.||||||
16873|Sidling sandstone""|69875|5|Briefly described|p264-266, p269|||Powell et al. (1993); in their Mathinna Group. Assigned to Panama Group (Mathinna Supergroup) by Reed (2001). Spelling changed, and unit formalised, as Sideling Sandstone by Seymour et al. (2010). Several kilometres thick.||||Overlay Bellingham Formation. Was overlain by St Marys Porphyrite.|Indurated quartzose sandstone, with poorly developed or no cleavage. Typical turbidite-type sedimentary structures common.|
74071|Simmonds Hill Metamorphics|61395|4|Described|p49-50, p76|||Of Green (1959). Recent mapping has discovered exposures of similar rocks in a fault-bound window through allochthonous Proterozoic Badger Head Gp sedimentary rocks which may lead to revised nomenclature in the future.||||||07-FEB-11
74071|Simmonds Hill Metamorphics|69874|4|Described|p107 Fig 4.9, p137, p138 Fig 4.37|Cambrian|Cambrian|Gee and Legge (1971, 1070). Also shown as Simmonds Hills metamorphic rocks (p107 Fig 4.9). Reed et al. (2002) argued these should be in Port Sorell Formation based on geochemistry. However their whole rock geochemistry is not definitive, metamorphic grade matches Settlers Schist closely and contrasts with very low grade Port Sorell Formation, so correlation is tenuous.||Andersons Creek Ultramafic Complex||Underlies Badger Head Group (now superseded by correlate Oonah Formation) structurally. Overlies Andersons Creek Ultramafic Complex.|Allochthonous metamorphic schist similar to Settlers Schist and a small block of amphibolite. Meta-sedimentary and meta-igneous rocks.|
35842|Simmonds Hill metamorphics|12179|6|Mentioned|p974|||Nomenclature of Green (1959). Superseded; see Settlers Schist.||||||
35842|Simmonds Hill metamorphics|23326|6|Mentioned|974|||Informal name - originally described by Green (1959). Now included in Settlers Schist.||||||18-APR-07
27568|Singing Creek Beds|39235|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16931|Singing Creek Siltstone|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tasmania.||||||04-OCT-07
16931|Singing Creek Siltstone|36047|5|Briefly described|p364|||||||||
16998|Slide Breccia|37412|6|Mentioned|Fig.2|||||||||
17004|Smelter Formation|42425|5|Briefly described|Table 2 P141, P150|||Variation/Misspelling of Smelters Limestone?||||||
17006|Smelters Limestone|40127|6|Mentioned|p10|||||||||
17006|Smelters Limestone|40136|5|Briefly described|p39|||||||||
17006|Smelters Limestone|44086|14|Not recorded|p99||Ordovician|See also Lexicon.||||||
17005|Smelters Limestone""|40136|6|Mentioned|p39|||||||||
17008|Smithton Dolomite""|42358|5|Briefly described|p11|||Used 1934, 1949. Correlated with Success Creek Group, Dundas Trough 1986.||||||
73351|Smithton basalt|63167|6|Mentioned|p14|Precambrian|Precambrian|Informal name (pers.comm: A.V. Brown; and. pers.comm: A.J. Crawford - no dates given).||||||04-OCT-07
68816|Smithton dolomite|24570|6|Mentioned|p396 Fig. 5, p397|Neoproterozoic III|Neoproterozoic III|Informal name.||||||
17010|Smithton dolomites|38638|6|Mentioned|p1901|||||||||
73350|Smithton volcanics|63167|5|Briefly described|p20|||Informal name.||||||
78548|Smithton-Trowutta Volcanics|67502|6|Mentioned|p73, p200-204 Tb.15b.|||Of Griffin (1974) who described the petrography and geochemistry of basalts (now the Spinks Creek Volcanics); he divided them into low-TiO2 and high TiO2 groups. His analyses are in Table 15b.||||||
73810|Sock Creek lava|638|5|Briefly described|p101|||Informal name. Overlies "Animal Creek Greywacke". Max. thickness: 200m. A unit of felsic lava with intercalations of siltstone, sandstone and breccia. Further details of lithology are included. ||||||
17113|South Comet Grit""|41795|6|Mentioned|p39|||||||||
70299|South Eastern Tasmania Granites|61723|6|Mentioned|p816|Devonian|Devonian|Informal collective term for the granites of southeastern Tasmania - including: Bicheno Granite, Deep Glen Bay Granite and Hippolyte Rocks Granite.||||||
30403|Southwell Sub-Group|23940|6|Mentioned|p920 Fig. 4|||Probably misspelt - see Southwell Subgroup.||||||
30403|Southwell Sub-Group|43135|5|Briefly described|Fig.2 p652|||Misspelling of Southwell Subgroup.||||||
79058|Spalford Conglomerate|69873|5|Briefly described|p87|||Of Burns (1964).||Unit in Ulverstone Metamorphics?|||Quartzite-derived, closed-framework, pebble to boulder grade conglomerate.|30-MAR-15
78556|Specimen Hill Siltstone|67502|6|Mentioned|p26|||Informally named by Yaxley (1981). Includes rocks now called Skinners Flat Siltstone. The Cassiterite Creek Quartzite corresponds to the upper member of this unit. See also Specimen Hill siltstone in this paper.||||||16-DEC-13
73338|Specimen Hill siltstone|63250|6|Mentioned|p9|||Informal name (Yaxley 1981). Repeated light grey, fine-grained siliceous sandstone to mainly siltstone beds grading upwards to dark grey weakly carbonaceous to quartzitic siltstone - striped appearance earned local name of "pyjama siltstone" (Veska 1993).||||||14-DEC-07
73338|Specimen Hill siltstone|67502|6|Mentioned|p25|||Informal, Yaxley (1981). Included the Skinners Flat Siltstone rocks. The Cassiterite Creek Quartzite corresponds to the upper member of this unit. See also Specimen Hill Siltstone in this paper.||||The Cassiterite Creek Quartzite corresponds to the upper member of this unit.||16-DEC-13
17155|Spero Bay Group""|41317|6|Mentioned|p170|||||||||
17156|Spero Bay lamprophyres|33354|6|Mentioned|p183|||Petrology.||||||
17157|Spero Group|33354|6|Mentioned|p186|||Lower Middle Dev.||||||
38770|Sprayton Beds|23837|6|Mentioned|p440 Fig.2|||||||||
79510|Sprent conglomerates|69874|5|Briefly described|p169, p171|||W of Lake Isandula, Dial Range Trough. Detritus was supplied from the Barrington Chert and the Motton Spilite.|||||Conglomerates rich in allochthon-derived chert and basalt detritus; some intercalated units of volcaniclastic sandstone and mixed provenance sandstone. Unfossiliferous.|
17184|Spreyton Beds|30150|6|Mentioned|Fig.5|||||||||
17184|Spreyton Beds|30155|6|Mentioned|p457|||||||||
17184|Spreyton Beds|30819|6|Mentioned|p108|||||||||
17184|Spreyton Beds|35288|6|Mentioned|p54|||||||||
17184|Spreyton Beds|36788|6|Mentioned|Fig.4|||||||||
17184|Spreyton Beds|43084|5|Briefly described|p141|Early Permian|Early Permian|Overlain by Mersey Coal Measures.||||||
17185|Spreyton Coal Measures|34323|6|Mentioned|p121|Permian|Permian|Should be Spreyton beds.||||||14-MAY-08
17186|Spreyton Formation|42000|6|Mentioned|Fig4 P59|||||||||
17197|Spring Sandstone|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
17197|Spring Sandstone|42349|5|Briefly described|Fig.3 P64|||See also Springs Sandstone in text P64. Misspelling of Springs Sandstone?||||||
17214|Springmount Formation|24549|4|Described|p6|Permian|Permian|Of the Ferntree Group. Max Thickness: 280ft||||||08-OCT-07
17214|Springmount Formation|30156|6|Mentioned|p40|||Part of Bogan Gap Group.||||||08-OCT-07
17214|Springmount Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Of the Ferntree Group.  Banded, grey micaceous quartz sandstone.||||||06-FEB-08
17214|Springmount Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
17217|Springmount Siltstone|30889|6|Mentioned|p46|||||||||
17216|Springmount Siltstone""|30889|6|Mentioned|p50|||||||||
74584|Springs Formation|63868|6|Mentioned|p17|||Term 'formation' used in grouping together several named units and is therefore probably an informal name.||||||07-FEB-11
17219|Springs Sandstone Formation|30819|6|Mentioned|p108|||||||||
29016|Sqirrel Creek Formation|37801|6|Mentioned|p113|||||||||
34174|St Marys Porphyrite|61216|5|Briefly described|p9, p20 Fig. 7a|||Included in the Scamander Tier Phase - Deformation D3. Two zones: Zone A - a lower, 800m-thick, compacted tuff ; Zone B: an upper vesiculated intrusive rock.Zone A conformable on thin breccia zone conformably overlying Mathinna Supergroup See also p41-42||||||10-FEB-11
34174|St Marys Porphyrite|61723|6|Mentioned|p823|Early Devonian|Early Devonian|Age: 388+/-1Ma (Rb-Sr).  Saint is St in text.||||||03-OCT-07
34174|St Marys Porphyrite|63170|5|Briefly described|p234, p235 Fig. 6.15|||Volcanic rocks with an age of 388+/1Ma. See also p236.||||||07-FEB-11
34174|St Marys Porphyrite|63635|5|Briefly described|p39||Early Devonian|Includes rhyolite.||||||
34174|St Marys Porphyrite|65646|6|Mentioned|p11, p36-38.|||Unit in, or co-genetic with Blue Tier batholith. Has 2 units: zone A, 800m of compacted tuff below Zone B, a vesiculated intrusive. Phenocrysts, typically fragmented, comprise up to 58% of the volume. Groundmass recrystallisation is widespread in Zone A.||||||09-JAN-15
34174|St Marys Porphyrite|66172|14|Not recorded|23|||Intrudes Scamander Slate and Quartzite.||||||09-SEP-10
34174|St Marys Porphyrite|66575|5|Briefly described|p953-954 Tb.3, Fig.14-15; p957 Fig.18|||I-Type; mafic, unfractionated. Presumably the same as St Marys Porphyry (p936 Fig.2, p955, p964 Fig.20). Nd-Sr, Pb isotope analyses.||||||
34174|St Marys Porphyrite|67493|6|Mentioned|p7, p9, p76|Givetian|Givetian||388 +/- 1 Ma (Turner et al. 1986).|||Unconformably overlies the Panama Group||
34174|St Marys Porphyrite|67503|4|Described|p6-12, 18, 36, 39, 41, 50, 54, 69, 72-3|Givetian|Givetian|~1400 m thick. Geochemistry and mineralogy support comagmatism (Blue Tier Batholith I-type linked) of St Marys Porphyrite, Catos Creek Dyke and Scamander Tier Dyke. Intruded along F1 thrusts, post-dates country rocks major tectonic structures. Mylonitic shears present.|388 +/- 1 Ma Rb-Sr and K-Ar (Turner et al. 1986).|||Intrudes the sediments of the Mathinna Supergroup.|Predominantly dacitic, welded, ash flow tuff with the vesiculated part of a volcanic feeder.|
34174|St Marys Porphyrite|67655|5|Briefly described|p19|Middle Devonian|Middle Devonian||388 +/- 1 Ma (Turner et al., 1986)||||Body of thick welded tuff, of dacite to rhyolite composition.|28-MAY-14
34174|St Marys Porphyrite|69871|5|Briefly described|p7|Devonian|Devonian||||||Granite-like caldera eruption.|
34174|St Marys Porphyrite|69875|5|Briefly described|p264 Fig 5.16, p266|Givetian|Givetian|Baillie et al. (1989).|388 +/- 1 Ma (Turner et al., 1986).|||Overlies Sideling Sandstone (Mathinna Supergroup) unconformably.|Ashflows and intrusives.|
34174|St Marys Porphyrite|69876|4|Described|p273-274, p277|Middle Devonian|Middle Devonian|Part of Blue Tier Batholith. See also references to St Marys Porphyry (p301, p304, p314). Scamander Tier and Catos Creek granodiorite dykes are considered to be intrusive equivalents. Pyroxene is pseudomorphosed by amphibole at higher levels; in hypabyssal equivalent micro-granodiorite body, both orthopyroxene and clinopyroxene remnants are found in amphibole cores.|388 +/- 1 Ma (Turner et al., 1986).|Scamander Tier Suite||Intrudes Mathinna Supergroup.|Large-scale I-type granitoid intrusion-related pyroclastic unit. Dacitic, welded ash-flow tuff of plagioclase, quartz, biotite, augite, hypersthene and sanidine phenocrysts in aphanitic groundmass.|
17265|Stanley Beds|42358|6|Mentioned|p27|||Misspelling of Stanley beds?||||||
17265|Stanley Beds|65653|6|Mentioned|p34.|||Poorly sorted pyroclastic basaltic sandstone, breccia and conglomerate up to 15 m thick. Intruded by basanitic dykes. ||||||
17265|Stanley Beds|69879|5|Briefly described|p463|Cenozoic|Cenozoic|Surrounds The Nut (Circular Head) at Stanley.|||||Pyroclastics.|
30397|Sticht Range Bed|43131|6|Mentioned|p583|||Misspelling of Sticht Range beds.||||||
17330|Sticht Range Beds|23947|6|Mentioned|p1074 Fig.1|||||||||
17330|Sticht Range Beds|23948|5|Briefly described|p1094 Fig.3|Middle Cambrian|Middle Cambrian|Of the Mount Read Volcanics.||||||
17330|Sticht Range Beds|40890|6|Mentioned|p50|||||||||
17330|Sticht Range Beds|41143|5|Briefly described|p271|||||||||
17330|Sticht Range Beds|41756|6|Mentioned|Fig.1|||||||||
17330|Sticht Range Beds|43054|6|Mentioned|p9|||Refers to Corbett (1982)||||||
17330|Sticht Range Beds|43131|4|Described|p568|||Misspelling of beds.||||||
17330|Sticht Range Beds|43133|4|Described|p598|||||||||
17330|Sticht Range Beds|43242|5|Briefly described|Map Legend||Cambrian|||||||
17330|Sticht Range Beds|43244|5|Briefly described|Map Legend||Cambrian|Of Tyndall Group.||||||
17330|Sticht Range Beds|43245|6|Mentioned|Map Legend||Cambrian|should read Sticht Range beds.||||||
17330|Sticht Range Beds|43247|6|Mentioned|Map Legend||Cambrian|||||||
17330|Sticht Range Beds|44135|6|Mentioned|p13|Late Cambrian||Of Baillie (1989c). Informal - see Sticht Range beds. Mentioned in combination with Mt Read Volcanics, as possibly forming an eastern 'trough' margin in the Dundas Trough.||||||07-DEC-09
17330|Sticht Range Beds|63612|6|Mentioned|p2, p12, p13|||Include sandstone.||||||07-FEB-11
17330|Sticht Range Beds|64395|6|Mentioned|p171 Fig. 4|||See also Sticht Range beds.||||||07-FEB-11
17330|Sticht Range Beds|69857|5|Briefly described|Map legend|Cambrian|Cambrian||||||Siliciclastic sandstone-siltstone-conglomerate units of metamorphic derivation.|
17330|Sticht Range Beds|69859|5|Briefly described|Map legend|Furongian|Furongian|Elliott Bay-Queenstown-Rosebery region.||Unit in Mount Read Volcanics.|||Quartz-rich sandstone-siltstone-conglomerate units of metamorphic derivation.|
17330|Sticht Range Beds|69874|4|Described|p150-151,p153,p155-156,p183,p217,p231|Late Cambrian|Middle Cambrian|Along the margin of Tyennan Block. Variable thickness up to 1200m of discontinuous lenses of siliciclastics. Age from trilobites. Interpreted as locally derived clastic sedimentation at margin of rising Tyennan Block following collision-obduction event in early Middle Cambrian. Subsequently swamped by Mount Read Volcanics.||Basal Eastern Quartz-Phyric Sequence.||Underlies Eastern Quartz-Phyric Sequence. Overlies Tyennan Basement. Is intruded by Bonds Range and Elliott Point Porphyries.|Interbedded quartzite-clast pebble-cobble conglomerate, siliceous sandstone, micaceous grey siltstone, mudstone; derived from underlying rocks; generally upward fining. Interbedded volcaniclastic sandstone towards the top.|
17330|Sticht Range Beds|69876|5|Briefly described|p286|Late Cambrian|Middle Cambrian|See also Sticht Range beds (p290).||||Underlies Eastern Quartz-Phyric Sequence, Western Volcanosed Sequence. Overlies Crimson Creek Formation, Tyennan Metamorphics. Intruded by Murchison Granite.||
17330|Sticht Range Beds|70274|4|Described|p446-448|Late Cambrian|Middle Cambrian|Lithostratigraphic unit of the Mount Read Volcanics. Thickness: <500m. Generally occurs along eastern margin of MRV. Potentially the oldest lithostratigraphic unit of the MRV. Poorly preserved trilobite fossils indicate a Middle-Late Cambrian age (Baillie 1989).||Unit of Mount Read Volcanics.||Overlain conformably by Eastern Quartz-Phyric Sequence.|Basal succession of interbedded basement-derived siliciclastic and volcaniclastic rocks.|
17330|Sticht Range Beds|70753|5|Briefly described|p185|Middle Cambrian|Middle Cambrian|Up to 1200m thick. Fining-upwards, recording transition from fluvial to marine conditions.||||Is overlain by Eastern Quartz-Phyric Sequence.|Siliciclastic conglomerate, sandstone and minor siltstone.|
17330|Sticht Range Beds|73313|6|Mentioned|Map legend|Cambrian Series 3|Cambrian Series 3|Map unit includes Sticht Range Beds and correlates, Animal Creek Greywacke; description of dominantly siliciclastic sandstone and conglomerate of partly Precamrian (Tyennian) provenance. Tullah-Dial Range-Fossey Mountains region.||Mount Read Volcanics||||
17330|Sticht Range Beds|73320|6|Mentioned|Map legend|Cambrian Series 3|Cambrian Series 3|Dundas, Fossey Mountains and Dial Range Troughs. Map unit includes Sticht Range Beds, Animal Creek Greywacke, Miners Ridge Sandstone; description of quartz-rich sandstone-siltstone-conglomerate units of metamorphic derivation.||Mount Read Volcanics||||
29554|Sticht Range beds|638|5|Briefly described|p84, p105|Middle Cambrian|Middle Cambrian|Basal unit of the Tyndall Group. Max. thickness: 500m. Thick interbedded grey sandstone, micaceous siltstone and siliciclastic pebble to boulder grade conglomerate. See also p88 Fig. 4.2, p85 Fig. 4.1.||||||
29554|Sticht Range beds|42976|5|Briefly described|p265|||Variation on Sticht Range Formation?||||||
29554|Sticht Range beds|43164|4|Described|1||Cambrian|||||||
29554|Sticht Range beds|43241|5|Briefly described|Map Legend||Cambrian|||||||
29554|Sticht Range beds|43242|5|Briefly described|Map Legend||Cambrian|||||||
29554|Sticht Range beds|43243|5|Briefly described|Map Legend||Cambrian|||||||
29554|Sticht Range beds|43248|6|Mentioned|Map Legend||Cambrian|||||||
29554|Sticht Range beds|43249|6|Mentioned|Map Legend||Cambrian|||||||
29554|Sticht Range beds|44135|5|Briefly described|p16, p17|||See also Sticht Range Beds. Part of the Mount Read Volcanics forming a thin discontinuous basal sequence of clastic sedimentary rocks along the eastern margin of the volcanic belt.||||||07-DEC-09
29554|Sticht Range beds|63169|4|Described|p157 Fig. 5.2, p162|Middle Cambrian|Middle Cambrian|Geological Province: Dundas Trough - along the eastern margin of Mount Read belt. Discontinuous sequence of clastic sedimentary rocks referred to as Sticht Range beds and correlates.||||||08-APR-13
29554|Sticht Range beds|64395|5|Briefly described|p167, p174 Fig. 8.|Middle Cambrian|Middle Cambrian|Succession of siliciclastic sandstone, conglomerate + siltstone predominantly derived from Precambrian rocks below. Unconformable on Precambrian basement. Grades up into volcaniclastic rocks suggesting it may form basal unit of Mount Read Volcanics.||||||07-FEB-11
29554|Sticht Range beds|69876|6|Mentioned|p290|Middle Cambrian|Middle Cambrian|See also Sticht Range Beds (p286). Cross-section, gravity modelling.||||||
73267|Stitt Quartzite""|63238|6|Mentioned|p15|||Of the "Rosebery Group". ||||||
73267|Stitt Quartzite""|63240|5|Briefly described|p4|||Redesignated from "Rosebery Group" to marine Owen Group from fossil evidence and lithology.||||||14-MAY-07
17342|Stocker Formation|34316|5|Briefly described|p21 Fig.3|Early Permian|Early Permian|Of the Golden Valley Group. Tillitic conglomerate; interbedded sandstone/siltstone in places.||||||06-FEB-08
40982|Stocker's Tillite|24547|4|Described|p11|Early Permian|Early Permian|See also Stockers Tillite. Overlain by the Quamby Mudstone. Unconformably overlain by the Gordon Limestone. Maximum Thickness: 13.72m.||||||07-MAY-04
17343|Stockers Formation|24549|4|Described|p9|Permian|Permian|Of the Golden Valley Group. Max Thickness: 340ft. Tillitic conglomerate with pebbles of quartzites, slates and schists in groundmass of grey mica mudstone||||||08-OCT-07
17343|Stockers Formation|37926|6|Mentioned|p495|||||||||
17343|Stockers Formation|43021|6|Mentioned|p459|||||||||
17343|Stockers Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Carboniferous|Late Carboniferous|Informal - see Stockers Tillite.||||||07-FEB-11
17343|Stockers Formation|63263|5|Briefly described|p33 Fig. 7|||Should this be Stockers Tillite?||||||07-FEB-11
40012|Stockers Glacial Formation|24548|5|Briefly described|Map 4687|Permian|Permian|||||||
17348|Stockton Tillite|40636|6|Mentioned|p44|||||||||
17354|Stockyard Tillite|36207|6|Mentioned|Text Fig.2|||||||||
17368|Stoney Creek Granite Porphyry|41142|6|Mentioned|Fig.1|||||||||
17370|Stoney Creek granitic porphyry|41142|5|Briefly described|p320|||||||||
17370|Stoney Creek granitic porphyry|41143|6|Mentioned|p273|||||||||
83036|Stoney Head Sandstone|73186|5|Briefly described|p228, p229, p230, p232, p239-240, p243|Floian|Floian|Lachlan Orogen, Eastern Tasmanian Terrane. Lower part of the Tippogoree Group, 1km thick. Geochemistry samples include a grey slate.  426.7 +/- 2.4 Ma Ar-Ar plateau age for dominant cleavage at Lefroy. Recumbent folding also attributed to Benambran deformation based on U-Pb monazite and xenotime ages in Turqoise Bluff Slate. [Misspelling of Stony Head Sandstone?, written as Stony Head Sandstone on p228]|426.7+/-2.4 Ma Ar/Ar deformation.|Tippogoree Group||Underlies the Industry Road Member.|Thick, graded beds of medium to fine-grained sandstone, typical of proximal turbidites.|
83036|Stoney Head Sandstone|73489|6|Mentioned|p655, p662|||See also Stony Head Sandstone.||Mathinna Supergroup||||
17478|Styx Formation|41908|6|Mentioned|p49|||Reserved as Styx Dolomite.||||||08-OCT-07
17480|Styx River Coalmeasures|31577|6|Mentioned|p90|||Plant fossils||||||
17482|Styx River complex|37056|6|Mentioned|p502|||||||||
77501|Success Creek Formation|61411|6|Mentioned|p6.|||Of Brown in Burrett & Martin, 1989.||||||01-NOV-12
77501|Success Creek Formation|70025|6|Mentioned|p4|Cryogenian|Cryogenian|Burnie Zone. Abbreviated as SC on p4 Fig 2. Underwent moderate to mild deformation. [Same stratigraphic unit as Success Creek Group?]||||||
17489|Success Group|38157|6|Mentioned|p287|||||||||
17489|Success Group|40760|6|Mentioned|p167|||||||||
17489|Success Group|43054|6|Mentioned|p31|||Misspelling of Success Creek Group?||||||
17489|Success Group|43595|5|Briefly described|p552||Neoproterozoic|||||||
83230|Suprise Bay Formation|73313|5|Briefly described|Map legend|Ectasian|Ectasian|King Island.|||||Micaceous quartzite, schist, phyllite and minor amphibolite.|
17587|Swifts Sandstone|42000|6|Mentioned|p69|||||||||
17621|Table Cape Beds|36119|6|Mentioned|p52|||||||||
17621|Table Cape Beds|48846|14|Not recorded|p6,15-21,26|||||||||
17622|Table Cape Conglomerate|35288|6|Mentioned|p41|||Reference Etheridge 1883. Superseded by Wynyard Tillite.||||||
17622|Table Cape Conglomerate|37926|6|Mentioned|p495|||||||||
27239|Tamarian Stage|30150|2|Defined|p95|early Sakmarian|early Sakmarian|||||||
27239|Tamarian Stage|38906|4|Described|p13|||||||||
27239|Tamarian Stage|38908|6|Mentioned|p6|||||||||
27239|Tamarian Stage|39680|6|Mentioned|Map legend|Permian|Permian|||||||
17884|Tasmanian Dolerites|24424|6|Mentioned|p543|Triassic|Permian|||||||
17884|Tasmanian Dolerites|33023|6|Mentioned|p321|||||||||
17884|Tasmanian Dolerites|34922|6|Mentioned|p365|||||||||
17884|Tasmanian Dolerites|34923|6|Mentioned|p366|||||||||
17884|Tasmanian Dolerites|36447|6|Mentioned|p91|||||||||
17884|Tasmanian Dolerites|39578|6|Mentioned|p112|||||||||
17884|Tasmanian Dolerites|42331|4|Described|p842|||||||||
17885|Tasmanian dolerite|23328|6|Mentioned|1036||Jurassic|Geochemical analysis given for comparison.||||||07-SEP-09
17885|Tasmanian dolerite|32106|6|Mentioned|p305|||Palaeomagnetic data||||||
17885|Tasmanian dolerite|32108|6|Mentioned|p232|||||||||
17885|Tasmanian dolerite|35895|6|Mentioned|Table 1|||||||||
17885|Tasmanian dolerite|36019|5|Briefly described|p932|||||||||
17885|Tasmanian dolerite|36551|6|Mentioned|p12|||||||||
17885|Tasmanian dolerite|40263|6|Mentioned|Table 2|||[Originally entered for NSW. CEBMar95]||||||
17885|Tasmanian dolerite|40268|6|Mentioned|p107|||[Originally entered for NSW||||||
17885|Tasmanian dolerite|69878|5|Briefly described|p392-393, p403-404, p406|Jurassic|Jurassic|Synonymous with Jurassic dolerite. Possible source materials discussed. Precedes the separation of Australia and Antarctica by some 85 m.y. K/Ar age range from whole rock samples and mineral separates from 5 widely separated localities.|183-156 Ma (Schmidt and McDougall, 1977).||||Dolerite.|
17886|Tasmanian tasmanite|40163|6|Mentioned|p361|||||||||
17887|Tasmanite Oil Shale|24547|5|Briefly described|p9, p26|||Of Newton (1875). Same as Bakes Oil Shale (Wells, 1957). Referred to as Tasmanite in text.  Maximum Thickness: 1.4m.||||||09-OCT-07
17887|Tasmanite Oil Shale|24552|5|Briefly described|p7|||Within base of Woody Island Formation and Quamby Formation.||||||07-FEB-11
17887|Tasmanite Oil Shale|30156|6|Mentioned|p38|||Occurs near base of sequences occupying same stratigraphic position as Quamby Mudstone.||||||09-OCT-07
17887|Tasmanite Oil Shale|34012|6|Mentioned|Map legend|Permian|Permian|Part of Quamby Mudstone.||||||09-OCT-07
17887|Tasmanite Oil Shale|35288|6|Mentioned|p47|||||||||
17887|Tasmanite Oil Shale|36788|6|Mentioned|p32|||||||||
17887|Tasmanite Oil Shale|37102|6|Mentioned|p264|||||||||
17887|Tasmanite Oil Shale|43084|5|Briefly described|p141||Late Carboniferous|||||||
17887|Tasmanite Oil Shale|69877|5|Briefly described|p364 Fig.7.1, p367, p382|Carboniferous|Carboniferous|Formed from the green alga Tasmanites punctatus. Occurs locally, 10-30m above the top of the basal diamictites. Contains the brachiopod Grumantia costellata (early Tamarian age). Excellent potential source rock for hydrocarbons, with high TOC values.||Unit in Woody island Formation.||||
17887|Tasmanite Oil Shale|70194|6|Mentioned|p297, p299, p300|Early Permian|Late Carboniferous|Mined 1910-1935.||Of Woody Island Formation.|||Black shale.|
17888|Tasmanite Shale|30155|6|Mentioned|p457|||||||||
17889|Tasmanite oil shale|36788|6|Mentioned|p105|||||||||
29049|Tasmanites oil shale|35288|6|Mentioned|p65|||Misspelling? of Tasmanite.||||||09-OCT-07
42324|Taswegian Granites|24270|6|Mentioned|p1614|||Geological Province: Lachlan Fold Belt.||||||
42324|Taswegian Granites|24512|6|Mentioned|p7|||Probably an informal name. See also Taswegian granites.||||||
68801|Taswegian granites|24512|6|Mentioned|p7|||Probably informal. See also Taswegian Granites.||||||
78300|Tayatea Dyke Swarm|67502|4|Described|p41-42|Proterozoic|Proterozoic|Replaces Rocky Cape Dyke Swarm. Specific dykes at Dempster Plains and Frankland River discussed.||||Intrudes Rocky Cape Group.|Dolerite, mainly tholeiitic, dykes.|07-JAN-15
78300|Tayatea Dyke Swarm|68241|6|Mentioned|p13|||Petrologically and geochemically broadly similar to tholeiitic metadolerite beach boulders on Albatross Island.||||||
78300|Tayatea Dyke Swarm|68243|6|Mentioned|p651|Ediacaran|Ediacaran|Of Brown 1989.|ca. 588-600 Ma|||||
78300|Tayatea Dyke Swarm|69857|5|Briefly described|Map legend|Cryogenian|Cryogenian||||||Tholeiitic dolerite dykes.|
78300|Tayatea Dyke Swarm|69873|4|Described|p54-56, p58 Fig.3.27, p70, p72-74, p85|Neoproterozoic|Neoproterozoic|Everard et al. (2007). NNE-NE-trending dykes, typically 10-50m, locally over 100m, wide and traceable for tens of kilometres. Geochemistry detailed: incompatible element spidergrams and REE plots, composition and fractionation trend diagrams. Possibly coeval, but certainly not comagmatic, with Bernafai and Spinks Creek Volcanics. Possible equivalent to Gairdner and Amata dyke swarms on the mainland. Described as crustally contaminated.|c.600 Ma or older.|||Intrudes Rocky Cape Group.|Tough, massive, usually aphanitic, dark grey-green to blue-grey dolerite; some more felsic dykes are coarser-grained and granophyric.|
73438|Taylor's Formation 1|63168|6|Mentioned|p79|Middle Cambrian|Middle Cambrian|Informal name of Taylor (1954) refers to a specific unnamed unit of the Huskisson Group. Mixture of metasedimentary and volcaniclastic materials, including volcanic detritus derived from andesitic and dacitic lavas and tuffs.||||||16-JUL-07
77498|Teatree Megabreccia|61411|6|Mentioned|p6.|||See Teatree Point Megabreccia.||||||
77498|Teatree Megabreccia|61412|6|Mentioned|p8, p10 Fig.6.|Middle Cambrian||Strongly sheared zone including blocks of chert, limestone and conglomerates. See Teatree Point Megabreccia.||||||
73439|Teatree Point Megabreccia|63168|5|Briefly described|p81|Cambrian|Cambrian|Of Burns (1964). Thickness: ~150m. Geological Province: along western margin of Dial Range Trough. Consists blocks of chert and other lithologies set in a matrix of lithic wacke and conglomerate.||||||
73439|Teatree Point Megabreccia|69874|5|Briefly described|p170-171, p184|Middle Cambrian|Middle Cambrian|Penguin area, North Coast Tasmania. Appears as Tea Tree Point Megabreccia on p170-171. Extension-related. 250m wide outcrop; allochthonous basalt on either side.||||Abuts Motton Spilite to E and W.||
79597|Tebrakunna Dyke Swarm|69876|4|Described|p319-321|Carboniferous|Devonian|Petrologically distinct from Jurassic Dolerite. Most common north of St Helens (inland of The Gardens). At least 20 subparallel NNE-trending dolerite dykes form a swarm 20km wide; individually up to 6km long, 1-30m wide, usually subvertical. Some outlying dykes mentioned. Magnetic anomalies suggest the swarm extends 80km in arcuate pattern. Diffuse/irregular margins suggest magma mingling or assimilation of country rock. Geochemistry, mineralogy described. Age constraints discussed.|Between c.377 Ma and c.335 Ma.|||Intrudes Lottah, Grants Point Granites; Bluestone Bay Granodiorite; and Mathinna Supergroup.|Dolerite dykes; aphyric or with sparse plagioclase phenocrysts in fine- to medium-grained subophitic, to less commonly intergranular, groundmass. Local marginal zones of (garnetiferous) quartz-feldspar porphyry.|
18045|The Patriachs Granite|42726|5|Briefly described|map legend|Middle Devonian||Misspelling of Patriarch.||||||
69606|Thirstane Basalt|61155|5|Briefly described|p19|Early Oligocene|Middle Eocene|Thickness: 175m. In Central North Tasmania.||||||
24025|Thirsty Lagoons granite|36374|4|Described|p61|||||||||
40013|Thompson Slate and Greywacke|24548|5|Briefly described|Maps 4687 and 46-88|Cambrian|Cambrian|Of the Dundas Group. Informal name - see Thompson Formation.||||||09-OCT-07
33460|Three Hummock Island Adamellite|44105|4|Described|p256|||Of the Interview Suite (p259).||||||26-SEP-07
83243|Three Hummock Island granite|73369|4|Described|p311, 313, 316, 331|||Radiometric K-Ar emplacement age 335 m.y.|||||Light coloured adamellite with abundant plagioclase phenocrysts up to 3 inches in size.|
18108|Thureau formation|41993|6|Mentioned|p7|||||||||
18140|Tiers Sandstone|45042|6|Mentioned|p13|||Triassic. See Plate 1||||||
18141|Tiers Shale|34010|6|Mentioned|Cor. chart|||Middle- Upper Triassic.||||||09-OCT-07
40352|Tiger Group|23923|5|Briefly described|p1216|Early Devonian|Ordovician|||||||
18154|Tim Shea Conglomerate|31461|6|Mentioned|p47|||||||||
18154|Tim Shea Conglomerate|38070|6|Mentioned|Fig.6|||p95||||||07-SEP-22
18153|Tim Shea Conglomerate""|30277|6|Mentioned|p213|||Refers Opik(1951),Banks(1962).||||||09-OCT-07
74382|Tim Shea Formation|63170|6|Mentioned|p186|||Probably misspelt and should be Tim Shea Sandstone.||||||07-FEB-11
18155|Tim Shea Sandtone|30275|6|Mentioned|p112|||||||||
18156|Tim Shea sandstone|41793|6|Mentioned|p60|||||||||
83501|Tim-Shea Sandstone|73489|5|Briefly described|p653|Early Ordovician|Furongian|Central Tasmania. Misspelling of Tim Shea Sandstone.||||Overlies Great Dome Sandstone, underlies Florentine Valley Formation|Sandstone.|
18172|Timboon Sand|22875|5|Briefly described|p14|Paleocene|Paleocene|Wangerrip Group||||||
18172|Timboon Sand|30578|5|Briefly described|p7|||||||||
18172|Timboon Sand|31372|6|Mentioned|p17|||||||||
18172|Timboon Sand|41185|6|Mentioned|Fig.4|||||||||
18172|Timboon Sand|41704|6|Mentioned|Fig.3|||||||||
18172|Timboon Sand|41868|6|Mentioned|p548|||||||||
18172|Timboon Sand|42318|5|Briefly described|p7|||||||||
18172|Timboon Sand|42361|6|Mentioned|p16|||Abbreviation of Timboon Sandstone?||||||
18172|Timboon Sand|42524|5|Briefly described|Fig.3 P27|||||||||
18172|Timboon Sand|42555|6|Mentioned|p285|||||||||
18172|Timboon Sand|42599|5|Briefly described|Fig.3 P614|||||||||
18172|Timboon Sand|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
18172|Timboon Sand|43171|6|Mentioned|5-8|||Of Sherbrook Formation. Age: 65-100Ma||||||
18172|Timboon Sand|43208|5|Briefly described|map legend|Maastrichtian|Campanian|Of Sherbrook Group.||||||
18172|Timboon Sand|43493|6|Mentioned|32||Late Cretaceous|||||||
18172|Timboon Sand|43744|6|Mentioned|Fig.3,p3|||||||||
18172|Timboon Sand|61182|6|Mentioned|p18|||Informal reference to Timboon Sand Member as an independent unit.||||||
18172|Timboon Sand|63124|5|Briefly described|p48 Fig. 5.1|||Of Williamson et al (1987) - together with Curdies Formation replacing Timboon Sand Member. Now superseded by Timboon Sandstone. Geological Province: Otway Basin.||||||
18172|Timboon Sand|71437|6|Mentioned|p157|||[Abbreviation of Timboon Sand Member]||Of Paaratte Formation||||
37230|Timbs Group""|23990|5|Briefly described|p167|||Infomal name.||||||
83503|Timbs Sandstone|73489|6|Mentioned|p654 Tb.1|||Central Tasmania.|||||Includes sandstone, glauconitic sandstone.|
77772|Tipogoree Group|65646|5|Briefly described|p6.|Ordovician|Late Cambrian|Includes Stony Head Sandstone, Turquoise Bluff Slate. Deformed by NE-directed thrusting and folding by Delamerian Orogeny. Unconformably separated from Panama Group.||||||08-FEB-16
40418|Togari Group, lower|24604|6|Mentioned|p906|||Informal - see the Togari Group.||||||
40418|Togari Group, lower|44135|6|Mentioned|p37|||Informal - see Togari Group.||||||07-DEC-09
40418|Togari Group, lower|63250|6|Mentioned|p14|||Informal - see Togari Group. ||||||
73120|Togari Group, upper|44135|6|Mentioned|p37|||Informal - see Togari Group.||||||07-DEC-09
74085|Transition Beds, Lower|61395|5|Briefly described|p34|||A subdivision of the informal collective terms for the Salisbury Hill and Eaglehawk Gully Formations. Superseded by Salisbury Hill Formation.||||||07-FEB-11
74085|Transition Beds, Lower|64396|5|Briefly described|p211|Ordovician|Ordovician|Otherwise historically known as "Wet Beds" - probably now renamed? Merge upwards into the interbedded calcareous siltstone and limestone of Upper Trasition Beds. Transition Beds are host rocks for Au mineralisation in the Beaconsfield Goldfield.||||||08-DEC-08
74087|Transition Beds, Upper|61395|5|Briefly described|p35|||A subdivision of the informal collective terms for the Salisbury Hill and Eaglehawk Gully Formations. Superseded by Eaglehawk Gully Formation.||||||07-FEB-11
74087|Transition Beds, Upper|64396|5|Briefly described|p210 Fig. 2, p211|Ordovician|Ordovician|Lower Transition Beds merge upwards into these interbedded calcareous siltstone and limestone rocks. Transition Beds are host rocks for Au mineralisation in the Beaconsfield Goldfield; overlies Cabbage Tree Conglom., also here called Cabbage Tree Fm. ||||||
74084|Transition beds, Lower|61395|5|Briefly described|p32|||A subdivision of the informal collective terms for the Salisbury Hill and Eaglehawk Gully Formations. Superseded by Salisbury Hill Formation.||||||07-FEB-11
74084|Transition beds, Lower|69876|5|Briefly described|p343|Ordovician|Ordovician|(Hills, 1998). Informal name. Included in the Salisbury Hill Formation.||Salisbury Hill Formation||||
74086|Transition beds, Upper|61395|5|Briefly described|p33|||A subdivision of the informal collective terms for the Salisbury Hill and Eaglehawk Gully Formations.  Superseded by Eaglehawk Gully Formation.||||||07-FEB-11
74086|Transition beds, Upper|69876|5|Briefly described|p343|Ordovician|Ordovician|Hills (1998). Subsequently absorbed into the Eaglehawk Gully Formation.||Eaglehawk Gully Formation||||
29077|Trial Bay serpentinite|48760|6|Mentioned|p124|||||||||
26956|Trial Ridge Beds|22705|6|Mentioned|p803|Late Cambrian|Middle Cambrian|Parts overlain by Denison Group.||||||02-JUL-08
26956|Trial Ridge Beds|30274|5|Briefly described|p101|||Middle - Upper Cambrian ? age.||||||
26956|Trial Ridge Beds|30275|3|Fully described|p112|||||||||
26956|Trial Ridge Beds|30281|6|Mentioned|p8|||Refers Corbett (in press).||||||09-OCT-07
26956|Trial Ridge Beds|35791|6|Mentioned|Fig.2|||Middle and Late Cambrian correlation chart for Tasmania.||||||30-APR-07
26956|Trial Ridge Beds|39235|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
26956|Trial Ridge Beds|41793|3|Fully described|p40|||See also p41 and p63.||||||30-APR-07
26956|Trial Ridge Beds|41907|5|Briefly described|p37|||||||||
26956|Trial Ridge Beds|43777|5|Briefly described|p10|||||||||
26956|Trial Ridge Beds|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Geological Province: Adamsfield Trough.||||||22-JAN-08
26956|Trial Ridge Beds|67502|6|Mentioned|p100||Cambrian|Adamsfield Trough. Indicated biostratigraphic correlate of the Scopus Formation||||||
26956|Trial Ridge Beds|69573|6|Mentioned|p659, 661|||||||||
26956|Trial Ridge Beds|69859|5|Briefly described|Map legend|Furongian|Furongian|Adamsfield-Jubilee region.|||||Upper member consists of dominantly conglomerate and lithic sandstone.|
26956|Trial Ridge Beds|69874|4|Described|p135, p149, p151, p172, p184, p214|Series 3|Series 3|See also p235-236, p238. Adamsfield area. An east-facing sequence, 1100m thick. Contains ESE-WNW trending folds which are absent in the nearby Dundas Trough. Contains late Middle Cambrian - Boomerangian fossils. Tyler Creek Beds are considered equivalent.||||Faulted contact with eastern edge of Boyes River Ultramafic Complex. Overlies Island Road Formation. Underlies Denison Group, unconformably.|Conglomerate, sandstone and mudstone; fossiliferous.|
26956|Trial Ridge Beds|70753|5|Briefly described|p184, p189|Middle Cambrian|Middle Cambrian|Oldest fossiliferous unit in the Adamsfield Trough. Up to 500m thick. Agnostoid and trilobite species listed. Undescribed fossils of similar age occur further to the S in Island Road and Boyd River Formations.||||Is overlain unconformably by the Singing Creek Formation (Denison Group).|Comprises a lower and an upper unit of resistant conglomerate and sandstone, separated by a fossiliferous unit of micaceous siltstones and sandstones.|
26956|Trial Ridge Beds|73320|5|Briefly described|Map legend|Furongian|Cambrian Series 3|Adamsfield - Jubilee region. Multiple map units include Trial Ridge Beds, Island Road Formation, Boyd River Formation, and possible correlates including Clytie Cove Group and Iron bound Group; descriptions of the map units are conglomerate-sandstone sequences, quartzwacke and lithicwacke turbidite with rare fossils in some sequences, quartz-rich conglomerate and sandstone.|||||Quartz-rich conglomerate and sandstone. Conglomerate and lithic sandstone in upper member.|
26956|Trial Ridge Beds|73489|5|Briefly described|p653|Miaolingian|Miaolingian|Central Tasmania.||||Underlies Singing Creek Formation|Volcanoclastic.|
26956|Trial Ridge Beds|75070|5|Briefly described|p178|Miaolingian|Miaolingian|Central Tasmania.||||Is overlain unconformably by Singing Creek Formation.|Sandstone, volcaniclastics.|
18583|Trial Ridge Beds""|41793|3|Fully described|p40|||||||||
18612|Trowutta Breccia|41908|6|Mentioned|p51|||||||||
18612|Trowutta Breccia|67502|6|Mentioned|p58 |||Jago (1981) used the term for some of the diamictite units (of the ?Kanunnah Subgroup).||||||
18611|Trowutta Breccia""|37933|3|Fully described|p551|||See also p549. Intended as informal name.||||||09-OCT-07
18611|Trowutta Breccia""|68243|6|Mentioned|p651|||Previously an informal description of the Julius River Member by Jago (1981).||||||16-DEC-13
78558|Trowutta Group|67502|6|Mentioned|p55, p58|||Of Matthews 1961. Informal, never formally defined. Equivalent to the Kanunnah Subgroup. Name avoided in this paper, as Jago (1981) used the term 'Trowutta Breccia' for some diamictite units in the same area.|||Salmon River Dolomitic Breccia Matthews (1961b)|||16-DEC-13
29691|Truro Formation|43021|6|Mentioned|p459|||Variation on Truro Tillite?||||||
29691|Truro Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Carboniferous|Late Carboniferous|Informal - see Truro Tillite.  See also p304 Fig. 8.7.||||||07-FEB-11
29691|Truro Formation|63263|5|Briefly described|p33 Fig. 7|||Probably misnamed and should be Truro Tillite?||||||07-FEB-11
18628|Tubicolar Sandstone|40127|6|Mentioned|p10|||||||||
18628|Tubicolar Sandstone|40136|6|Mentioned|p35|||See also p41.||||||09-OCT-07
18628|Tubicolar Sandstone|63170|6|Mentioned|p192|||Of Jennings 1963). Former name for Moina Sandstone.||||||07-FEB-11
18628|Tubicolar Sandstone|69875|5|Briefly described|p246|||See eg Twelvetrees (1913). Designated Moina Sandstone by Jennings (1958, 1963, 1979).||||Equivalent to Caroline Creek Formation.|Sandstone with abundant perpendicular burrows.|
18654|Tulendeena Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Tulendeena Granodiorite [M.McClenaghan Jan95]||||||
18654|Tulendeena Granite|61216|5|Briefly described|p20 Fig. 7a|||Presented as Tulendeena only in map of granites. Part of the Scottsdale Batholith.||||||10-FEB-11
18654|Tulendeena Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Diddleum Suite, Scottsdale Batholith.  I-type granite, mafic, unfractionated, reduced. Name implied from map legend.||||||25-SEP-07
18656|Tullah Suite|42209|6|Mentioned|Fig.4 P269|||||||||
18728|Turritella bed""|30877|6|Mentioned|p29|||Now Fossil Bluff Sandstone||||||
18739|Twin Creek Formation|42227|6|Mentioned|p22-23 Fig. 3, p24|||Misspelling of Twin Creeks Formation.||||||16-JUN-09
79512|Tyennan Complex|69874|6|Mentioned|p99|||Alternative name, see Forth Metamorphic Complex.||||||
83427|Tyennan Metasediments|69842|6|Mentioned|p4, 10-11|Proterozoic|Proterozoic|Kelly, Albina, Philips, Sarah, Table Head maps; rocks at Cape Sorell, Liberty Point, Table Headand Gorge Creek-Neilson River area, have been designated as this unit rather than Rocky Cape Group correlates as previously.||||||
34030|Tyennan Nucleus|22603|5|Briefly described|Fig.1,p98||Cryogenian|c. 800 Ma||||||
18748|Tyennan metamorphics|40890|6|Mentioned|Fig.2|||Misspelling of Tyenna? [or informal use?!]||||||
18748|Tyennan metamorphics|69876|5|Briefly described|p290, p294,313,315,323|Proterozoic|Proterozoic|Regional cross-section. Proterozoic basement underlying Crimson Creek Formation, Barrington Chert. Is intruded by Devonian and Cambrian granites. Tyennan nucleus 87Sr/86Sr ratios.||||Underlies Gordon Group, Owen Group, Sticht Range beds, Jane Dolomite.||
18750|Tyler Creek Beds|40714|3|Fully described|p61|||Age:||||||
18750|Tyler Creek Beds|41562|5|Briefly described|p525|||||||||
18750|Tyler Creek Beds|43777|5|Briefly described|p11|Late Cambrian|Middle Cambrian|||||||
18750|Tyler Creek Beds|69858|5|Briefly described|Map legend|Cambrian|Cambrian||||||Lithicwacke and conglomerate with ultramafic detritus.|
18750|Tyler Creek Beds|69874|4|Described|p136-137,p149,p151,p173,p184,p214,p238|Late Cambrian|Middle Cambrian|South Coast area, east of New River Lagoon. Represents an unstable melange-like proximal flysch sequence, over 300m thick. Contains overturned folds and major NE-striking shear zones which predate the Denison Group. Mostly unfossiliferous, apart from some Middle to Late Cambrian sponge spicules. Presumed source of chromite and traces of osmiridium in black sands at Osmiridium Beach, probably reworked from conglomeratic serpentinite clasts.||||Overlies Rocky Boat Harbour Ultramafic Complex. Underlies Point Vivian Formation unconformably. Considered equivalent to Trial Ridge Beds.|Distinctive red and green polymict conglomeratic beds with abundant serpentinite and dolomite clasts; interbedded with graded sandstones and mudstones.|
18750|Tyler Creek Beds|70753|5|Briefly described|p184, p189|Late Cambrian|Middle Cambrian|Berry and Harley (1983), Bischoff (1983). Rocky Boat Inlet-Surprise Bay area. Only fossil is a sponge spicule.||||Is overlain unconformably by Point Vivian Formation. Suggested correlation with Trial Ridge Beds.|Serpentinitic conglomerate, sandstone and mudstone.|
38670|Tyndal Group|23786|5|Briefly described|p50|Cambrian|Cambrian|Of Mount Read Volcanics - name probably misspelt?||||||25-OCT-07
38670|Tyndal Group|73430|6|Mentioned|p518|Cambrian|Cambrian||510-493 Ma|||Unconformably overlain by Dennison Supergroup||
40525|Tyndall Complex, Lower|23948|6|Mentioned|p1103 Fig.9|||Informal name - see Lynchford Member.||||||
40525|Tyndall Complex, Lower|60424|5|Briefly described|p365|||Informal name.  Volcaniclastic sequence containing fossiliferous limestone lenses and hydrothermal carbonate.||||||27-SEP-07
18753|Tyndall Group ignimbrite|39892|5|Briefly described|p28|||||||||
18754|Tyndall Group lavas|37045|6|Mentioned|p225|||||||||
18755|Tyndall Group slate|39892|5|Briefly described|p28|||||||||
40526|Tyndall Group, Lower|23948|5|Briefly described|p1094 Fig.3|Middle Cambrian|Middle Cambrian|Informal - see Tyndall Group. Maximum Thickness: 150m||||||
40526|Tyndall Group, Lower|63675|6|Mentioned|p13 Fig.8|Middle Cambrian|Middle Cambrian|Includes Lynchford Member. Breccia complex with lenses of limestone and sulfides.||||||
40526|Tyndall Group, Lower|67655|5|Briefly described|p13 Fig. 8||||||Lynchford Member|||
40526|Tyndall Group, Lower|69874|5|Briefly described|p166, p202-204, p206|Middle Cambrian|Middle Cambrian|Simplified nomenclature for the basal breccia-rich facies component of the Tyndall Group; used by Corbett (2001).||||||
40527|Tyndall Group, Middle|23948|5|Briefly described|p1094 Fig.3|Middle Cambrian|Middle Cambrian|Informal - see the Tyndall Group.||||||
40527|Tyndall Group, Middle|63675|6|Mentioned|p13 Fig.8|Middle Cambrian|Middle Cambrian|Mostly volcaniclastic sandstone and conglomerate.||||||
40527|Tyndall Group, Middle|67655|5|Briefly described|p13 Fig. 8||||||||mostly volcaniclastic sandstone and conglomerate|
40527|Tyndall Group, Middle|69874|5|Briefly described|p166, p202-204, p206|Middle Cambrian|Middle Cambrian|Simplified nomenclature for the banded crystal-rich sandstone facies component of the Tyndall Group; used by Corbett (2001).||||||
39947|Tyndall Group, Upper|23948|5|Briefly described|p1094 Fig. 3|Middle Cambrian|Middle Cambrian|Informal - see Tyndall Group.||||||17-JAN-07
39947|Tyndall Group, Upper|24265|6|Mentioned|p1456|||Geological Province: Tasman Fold Belt||||||
39947|Tyndall Group, Upper|63675|6|Mentioned|p13 Fig.8|Middle Cambrian|Middle Cambrian|Mostly volcaniclastic sandstone and conglomerate.||||||
39947|Tyndall Group, Upper|67655|5|Briefly described|p13 Fig. 8||||||||mostly volcaniclastic sandstone and conglomerate|
39947|Tyndall Group, Upper|69874|5|Briefly described|p166, p202-204, p206|Middle Cambrian|Middle Cambrian|Simplified nomenclature for the volcaniclastic conglomerate facies component of the Tyndall Group; used by Corbett (2001).||||||
70022|Tyndall Group, lower|61260|5|Briefly described|p412 Fig. 1|Middle Cambrian|Middle Cambrian|Informal - see Tyndall Group.||||||
69922|Tyndall Group, upper|61260|5|Briefly described|p412 Fig. 1|Late Cambrian|Late Cambrian|Informal - see Tyndall Group.||||||
73303|Tyndall conglomerates, upper|63238|6|Mentioned|p8|||Informal reference to conglomerates in the Tyndall Group. Also referred to as Tyndall Group conglomerates. ||||||
42036|Ugbrook Limestone Formation|50091|5|Briefly described|p407|Middle Ordovician|Middle Ordovician|Panderodus nogamii (conodont) found.  See also Ugbrook Member.||||||04-NOV-04
24627|Ugbrook Member|42478|5|Briefly described|Fig. 21 P19|||Misspelling/variation of Ugbrook Formation.||||||
24627|Ugbrook Member|50091|5|Briefly described|p413 Tb. 1|Late Ordovician|Middle Ordovician|Occurrence of Panderodus nogamii (conodonts) - in Mole Creek area (Tas).  See also Ugbrook Limestone Formation.||||||04-NOV-04
34213|Ulverstone Metamorphic Complex|12179|5|Briefly described|p974|||Nomenclature of Turner (1989). The boundary between the Forth and Ulverstone metamorphic complexes was identified arbitrarily on a metamorphic grade boundary, despite a continuum in structural history across the inlier (Burns 1964). Deemed obsolete in this study (Meffre  et al., 2000) as Ulverstone MC is deemed a high-strain lower-grade unit with close structural association to the Forth MC, and proposed to have Ulverstone MC included as part of the Forth MC. See Forth Metamorphic Complex.||||||
34213|Ulverstone Metamorphic Complex|22668|5|Briefly described|p24||Proterozoic|||||||
34213|Ulverstone Metamorphic Complex|23326|4|Described|974|||Of Turner (1989). Now included in Forth Metamorphic Complex.||||||18-APR-07
34213|Ulverstone Metamorphic Complex|23990|6|Mentioned|p184|||||||||
34213|Ulverstone Metamorphic Complex|60900|6|Mentioned|p887 Fig. 1, p888|Paleoproterozoic|Paleoproterozoic|Age: 1792+/-6Ma.  See also p892.||||||07-NOV-08
34213|Ulverstone Metamorphic Complex|63167|4|Described|p30-31|||Also referred to as Metamorphics. Overlies the Forth Metamorphic Complex with which it is structurally concordant. Consists of massive and flaggy quartzite with interlayered fine-grained, muscovite-chlorite schist and subordinate conglomerate.||||||27-FEB-13
34213|Ulverstone Metamorphic Complex|69873|6|Mentioned|p52|||Forth region. [Name superseded by Ulverstone Metamorphics]. Detrital zircon populations discussed.||||||
81981|Unicorn Point Granodiorite|71730|6|Mentioned|p27, 31,33, p35, p37, p43, p58|Devonian|Devonian|Low heat generation. Name implied from p43.|||||Unfractionated I-type granodiorite.|09-NOV-20
18858|Upper Blessington Granite|42726|5|Briefly described|map legend|Middle Devonian||Should be Upper Blessington Granodiorite [M.McClenaghan Jan 95]||||||
18858|Upper Blessington Granite|61216|5|Briefly described|p20 Fig. 7a|Middle Devonian|Middle Devonian|Presented as Upper Blessington only in map of granites.  Age: 388.9+/-1.6Ma. Part of the Scottsdale Batholith.||||||10-FEB-11
18858|Upper Blessington Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Russells Road Suite, Scottsdale Batholith.  I-type granite, mafic to felsic, unfractionated to weakly fractionated, reduced. Name implied from map legend.||||||25-SEP-07
18858|Upper Blessington Granite|69876|5|Briefly described|p304, p306 Tb 6.1|Middle Devonian|Middle Devonian|Scottsdale Batholith.|c.390-387 Ma (SHRIMP U-Pb).|Russells Road Suite.|||I-type.|
29090|Upper Freshwater Sequence|42331|4|Described|p844|||Unintentional formalisation of "Upper Freshwater Sequence"?||||||
29090|Upper Freshwater Sequence|69877|6|Mentioned|p363|Permian|Permian|Of Clarke and Banks (1975), who divided the (now Parmeener Supergroup) succession according to depositional environment. This unit did not include the thick non-marine Triassic rocks which constitute the bulk of what is now the Upper Parmeener Supergroup.||||||
18894|Upper Freshwater Sequence""|30819|6|Mentioned|p107|||||||||
18916|Upper Limestone Member|23187|5|Briefly described|Fig2p237,247|Bolindian|Eastonian|||||||
18916|Upper Limestone Member|42416|6|Mentioned|p194|||?informal Member of Benjamin Limestone.||||||
18916|Upper Limestone Member|42478|6|Mentioned|p7|||||||||
18916|Upper Limestone Member|69875|4|Described|p243 Fig 5.2, p251-255|Late Ordovician|Late Ordovician|Images and descriptions of fossils. Correlates with Precipitous Bluff beds; fossiliferous limestone on Picton River; Salisbury River below Vanishing Falls micrite, with calcareous mudstone, siltstone and dolomitic micrite, 40m unit with abundant Palaeofavosites. Geochemistry briefly described. Correlations with unnamed limestone outcrops listed.||Benjamin Limestone||Underlies Arndell Sandstone. Overlies Lords Siltstone Member.|Peritidal carbonates, dominantly micrite limestone, thicker than 5-20m thick cyclical prograding tidal flats.|
18920|Upper Marine Sequence""|30819|6|Mentioned|p107|||||||||
18920|Upper Marine Sequence""|69877|5|Briefly described|p363|Permian|Carboniferous|Of Clarke and Banks (1975), who divided the (now Parmeener Supergroup) succession according to depositional environment.|||||Fossiliferous marine siltstone and sandstone.|
18943|Upper Parmeener Super-Group|32059|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
18943|Upper Parmeener Super-Group|35818|4|Described|p9|||||||||
18943|Upper Parmeener Super-Group|35819|4|Described|p13|||||||||
18943|Upper Parmeener Super-Group|36787|6|Mentioned|Map legend|Triassic|Triassic|||||||
18943|Upper Parmeener Super-Group|37405|5|Briefly described|p29|||||||||
18943|Upper Parmeener Super-Group|39680|6|Mentioned|Map legend|Triassic|Triassic|||||||
18943|Upper Parmeener Super-Group|40694|4|Described|p15|||||||||
18943|Upper Parmeener Super-Group|43072|5|Briefly described|p25|||||||||
18943|Upper Parmeener Super-Group|69854|5|Briefly described|Map legend|||||||||
18944|Upper Parmeener Supergroup|73294|5|Briefly described|p1005, p1007|late Triassic|late Permian|Flat-lying, non-marine, dominantly sandy, fluvial succession less than 1km thick. Uppermost, Upper Triassic unit informally referred to as 'Unit 4' (Forsyth, 1987, 1989) or 'Volcanic lithic sandstone and coal measures' (Reid et al., 2014), formally designated as the Mount Nicholas Coal Measures in northeast Tasmania. Unit 3 is a Middle Triassic quartz sandstone-dominated unit including basalt with a K-Ar (whole-rock) age of 233 +/- 5 Ma (Calver and Castleden, 1981). Older parts (Units 1 and 2) are absent or relatively thin in northeast Tasmania.|233 +/- 5 Ma K-Ar (whole-rock)|Parmeener Supergroup|Mount Nicholas Coal Measures||Fluvial succession of lithic sandstone, mudstone and coal. Laterally variably. Includes a quartz sandstone-dominated unit with basalt. Volcanic lithic sandstone and coal measures in upper part.|
18944|Upper Parmeener Supergroup|73320|5|Briefly described|Map legend|Triassic|Permian|Underlies erosional surface. Alkali olivine basalt/hawaiite in St Marys area.||||Overlies Lower Parmeener Supergroup.|Contains fluviolacustrine sequences of sandstone, siltstone and mudstone; lithic volcaniclastic sandstone; lithic sandstone, siltstone, mudstone and felsic tuff with some coal and quartz sandstone; alkali olivine basalt/hawaiite.|
18944|Upper Parmeener Supergroup|73321|5|Briefly described|Map legend|Triassic|Permian|Freshwater depositional environment.|||Cygnet Coal Measures.|Overlies the Lower Parmeener Supergroup.|Includes predominantly cross-bedded quartzose to feldspathic sandstone and micaceous siltstone, minor thin beds of quartz-pebble conglomerate, a less feldspathic interval, areas of overturned cross-bedding, and subordinate micaceous siltstone.|
18944|Upper Parmeener Supergroup|73322|5|Briefly described|Map legend|Triassic|Permian|||||Overlies the Lower Parmeener Supergroup.|Includes undifferentiated volcaniclastic, quartz-rich lithic and quartzose sandstone, siltstone, mudstone, carbonaceous beds and coal seams; interbedded micaceous carbonaceous silstone, shale, mudstone and sandstone.|
18944|Upper Parmeener Supergroup|73323|5|Briefly described|Map legend|Triassic|Permian||||Cygnet Coal Measures, Knocklofty Formation, Poets Road Member, Newton Coal Measures|Overlies the Lower Permeener Supergroup.|Includes freshwater arkosic to quartzose sandstone, often cross-bedded; micaceous or carbonaceous siltstone, mudstone and shale; lithic sandstone, coal seams; fossil plants in places; contact metamorphosed by Jurassic dolerite.|
18944|Upper Parmeener Supergroup|73324|6|Mentioned|Map legend|Triassic|Triassic|||||||
18944|Upper Parmeener Supergroup|73325|5|Briefly described|Map legend|Triassic|Triassic||||Knocklofty Formation||Includes cross-bedded quartzose to feldspathic sandstone; micaceous and carbonaceous siltstone, shale, mudstone and thin beds of silicified bioturbated sandstone; quartz-rich lithic sandstone and quartz sandstone, some with quartz granules/pebbles.|
18944|Upper Parmeener Supergroup|73326|5|Briefly described|Map legend|Triassic|Permian||||Cygnet Coal Measures, Knocklofty Formation, Newton Coal Measures.|Overlies the Lower Parmeener Supergroup.|Includes freshwater arkosic to quartzose sandstone, some silicified; interbedded micaceous and carbonaceous siltstone, mudstone and shale; lithic sandstone, coal seams; fossil plants in places; in part contact metamorphosed by Jurassic dolerite.|
18944|Upper Parmeener Supergroup|73327|5|Briefly described|Map legend|Triassic|Permian||||Cygnet Coal Measures, Knoklofty Formation|Overlies the Lower Parmeener Supergroup|Includes freshwater, predominantly cross-bedded quartzose to feldspathic sandstone, micaceous siltstone, minor thin beds of quartz-pebble conglomerate, intervals of siltstone, shale, mudstone and sandstone.|
18944|Upper Parmeener Supergroup|73328|5|Briefly described|Map legend|Triassic|Triassic||||Knocklofty Formation, Newton Coal Measures.|Overlies the Lower Parmeener Supergroup.|Includes often interbedded micaceous and carbonaceous siltstone, shale and mudstone, quartzose, lithic and arkosic sandstones, some cross-bedded, and thin beds of silicified sandstone; contains coal seams, fossil plants and bioturbation in places.|
18945|Upper Parmeener lithic sandstone|30926|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
26970|Upper Parmeener quartzose sandstone|30926|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
24061|Vansittart Island granite|36374|5|Briefly described|p61|||||||||
24061|Vansittart Island granite|71730|6|Mentioned|p43|||Moderately high heat generation.||||||
19061|Varna Bay Granite Complex|33354|4|Described|p183|||||||||
29099|Varna Granite|33354|4|Described|p187|||Petrology & genesis||||||
19062|Varvoid Bay Group|37412|6|Mentioned|p26|||Name should no longer be used.||||||
73640|Vicarys Creek Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Gardens Suite, Blue Tier Batholith.  I-type granite, mafic, unfractionated, reduced. Name implied from map legend.||||||
73640|Vicarys Creek Granite|71730|6|Mentioned|p33, p35, p37, p56||||||||I-type granite.|
19119|View Coal Measures|38731|6|Mentioned|p26|||||||||
19166|Waarre Sandstone|22930|6|Mentioned|50|||||||||
19166|Waarre Sandstone|22932|6|Mentioned|22|||||||||
19166|Waarre Sandstone|22944|5|Briefly described|Fig3|Turonian|Cenomanian|||||||
19166|Waarre Sandstone|24056|5|Briefly described|p85|Late Cretaceous|Late Cretaceous|Of Sherbrook Group.  Max. thickness: 34m.  Geological Basin: Otway Basin.||||||
19166|Waarre Sandstone|24314|5|Briefly described|p61 Fig.2|Turonian|Cenomanian|Geological Province: Otway Basin. Max. Thickness 204m. Of the Shipwreck Subgroup.||||||30-NOV-04
19166|Waarre Sandstone|24562|5|Briefly described|p3, 8|Late Cretaceous|Late Cretaceous|Of the Sherbrook Group.  Geological Province: Otway Basin.||||||
19166|Waarre Sandstone|30578|5|Briefly described|p7|||||||||
19166|Waarre Sandstone|30675|5|Briefly described|p253|||Lithology and radioactivity.||||||16-OCT-07
19166|Waarre Sandstone|30905|6|Mentioned|Table 7.3|||||||||
19166|Waarre Sandstone|31036|1|Redefined|p199|Cretaceous|Cretaceous|See also p200, Table 9-1. Basal unit of Wangerrip Group.||||||16-OCT-07
19166|Waarre Sandstone|31424|4|Described|p19|||See also p7. Described from core.||||||16-OCT-07
19166|Waarre Sandstone|31534|6|Mentioned|p363|||See also Table 19-3. U.Cretaceous||||||
19166|Waarre Sandstone|31625|6|Mentioned|Fig. 5.2|||U.Cret.||||||
19166|Waarre Sandstone|32162|6|Mentioned|p59|||||||||
19166|Waarre Sandstone|32898|6|Mentioned|p29|||U.Cret. See also Table 2-1||||||
19166|Waarre Sandstone|33940|6|Mentioned|Fig.21-1|||Cenomanian - Turonian.||||||
19166|Waarre Sandstone|35013|6|Mentioned|p393|||||||||
19166|Waarre Sandstone|36913|6|Mentioned|p78|||||||||
19166|Waarre Sandstone|36916|6|Mentioned|p107|||||||||
19166|Waarre Sandstone|38625|6|Mentioned|Table 2|||||||||
19166|Waarre Sandstone|40560|5|Briefly described|Fig.3|||||||||
19166|Waarre Sandstone|41016|5|Briefly described|p214|||||||||
19166|Waarre Sandstone|41123|6|Mentioned|p179|||||||||
19166|Waarre Sandstone|41185|5|Briefly described|p177|||See also Fig.5||||||
19166|Waarre Sandstone|41642|4|Described|p244|||||||||
19166|Waarre Sandstone|41704|6|Mentioned|Fig.3|||||||||
19166|Waarre Sandstone|41868|6|Mentioned|p534|||||||||
19166|Waarre Sandstone|41936|6|Mentioned|p75|||||||||
19166|Waarre Sandstone|42152|4|Described|p13|||Also Briefly described p33.||||||16-OCT-07
19166|Waarre Sandstone|42361|3|Fully described|p13|||||||||
19166|Waarre Sandstone|42524|5|Briefly described|Fig.3 P27|||||||||
19166|Waarre Sandstone|42545|6|Mentioned|p19|||In the Otway Basin.||||||16-OCT-07
19166|Waarre Sandstone|42555|5|Briefly described|p284|||||||||
19166|Waarre Sandstone|42599|5|Briefly described|p613|||||||||
19166|Waarre Sandstone|42827|4|Described|p244|||see also Table 7.12, same as Waarre Formation||||||
19166|Waarre Sandstone|42863|5|Briefly described|Fig.14|||Variation on Victorian unit.||||||
19166|Waarre Sandstone|43171|6|Mentioned|7-8|||Of Sherbrook Group. Age: 90-95Ma. Formerly the informal Shipwreck Group.||||||16-OCT-07
19166|Waarre Sandstone|43195|5|Briefly described|Map Legend||Late Cretaceous|Of the Sherbrook Group.||||||16-OCT-07
19166|Waarre Sandstone|43252|5|Briefly described|p163|||||||||
19166|Waarre Sandstone|43814|6|Mentioned|Fig.3,p115|||||||||
19166|Waarre Sandstone|44133|4|Described|p146|Cenomanian|Cenomanian|Previously 'Waarre Formation' now redefined. Thickness: 108m. Of the Sherbrook Group. Geological Province: Otway Basin.||||||
19166|Waarre Sandstone|48581|14|Not recorded|p30|||||||||
19166|Waarre Sandstone|48911|6|Mentioned|Chart 1|||||||||
19166|Waarre Sandstone|60538|5|Briefly described|p474 Fig. 13|||Geological Province: Otway Basin.||||||
19166|Waarre Sandstone|61182|6|Mentioned|p15|Late Cretaceous|Late Cretaceous|Former name used for Waarre Formation. ||||||
19166|Waarre Sandstone|61547|6|Mentioned|p461 Fig.2, p462. |Turonian|Cenomanian|||Unit in Shipwreck Subgroup.||Overlies Copa Formation. Is overlain by Belfast Mudstone and Flaxman Formation.||
19166|Waarre Sandstone|61622|5|Briefly described|p436 Fig. 2|Cretaceous|Cretaceous|Sherbrook Group. Geological Province: Otway Basin.||||||07-FEB-11
19166|Waarre Sandstone|61627|5|Briefly described|p500 Fig. 2|Late Cretaceous|Late Cretaceous|Of Shipwreck Subgroup. Geological Province: Otway Basin.||||||07-FEB-11
19166|Waarre Sandstone|63122|5|Briefly described|p17 Fig. 4.3|Turonian|Cenomanian|Of the Sherbrook Group. Unconformable over Eumeralla Formation. Max. thickness: 204m. Geological Province: Otway Basin. ||||||
19166|Waarre Sandstone|63124|3|Fully described|p48 Fig. 5.1, p49 Fig. 5.2, p77|Cenomanian|Cenomanian|First used in 1965 (Bock and Glenie) and variously renamed Waarre Formation and Waarre Sandstone. Overlies Eumeralla Formation; underlies Belfast Mudstone. Max. thickness: 204m. Geological Province: Otway Basin.||||||
19166|Waarre Sandstone|63125|6|Mentioned|p121 Tb. 7.11, p123|||Geological Province: Otway Basin||||||
19166|Waarre Sandstone|63129|5|Briefly described|p127, p137|Late Cretaceous|Late Cretaceous|Overlies Copa Formation. Geological Province: Otway Basin.||||||30-JAN-08
19166|Waarre Sandstone|63269|5|Briefly described|p606-607, p616, p618|Late Cretaceous|Late Cretaceous|Thought to be the source of oil in Caroline-1. See also Waarre Formation (p605). Details of natural gas, oils and oil stains in named wells tabulated. Oil-source correlation. Biomarker diagram.||||||
19166|Waarre Sandstone|63431|5|Briefly described|p677 Fig. 2|Turonian|Cenomanian|Of the Shipwreck Subgroup (Sherbrook Group). Overlies Copa Formation. Geological Province: Penola Trough/Otway Basin.||||||07-FEB-11
19166|Waarre Sandstone|71437|4|Described|Fig. 1 opp 154, p155, p156-157, 159|Turonian|Albian|Subsurface. Formerly included with 'Otway Group'. Shallow-water marine to brackish-water sequence (Leslie 1965). Restricted to a small area near Port Campbell.||Of Wangerrip Group.||Transitional with overlying Flaxman Formation.|Well sorted mature quartz sandstone, minor mudstone.|
40015|Warner Laminated Siltstone|24548|5|Briefly described|Map 4687|Cambrian|Cambrian|Of the Dundas Group. Informal name - see Warner Siltstone. See also Deloraine Map 46-88.||||||10-OCT-07
73733|Wart Hill Pyroclastics""|63612|5|Briefly described|p8, p25|||Associated with the Western Volcano-Sedimentary Sequence in its eastern section - felsic volcanic breccia-sandstone containing sulphide clasts and several large blocks or lenses of massive Pb-Zn-rich sulphide giving rise to exploration at Elliott Bay||||||07-FEB-11
19547|Wart Hill pyroclastics|41143|6|Mentioned|p273|||||||||
19577|Waterfall Gully dyke|35844|4|Described|p44|||Petrology||||||
19578|Waterfall Valley Formation|23837|6|Mentioned|p440 Fig.2|||||||||
19578|Waterfall Valley Formation|30155|6|Mentioned|Fig.33.4|||||||||
19578|Waterfall Valley Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
19578|Waterfall Valley Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
73734|Waterloo Creek Group""|63612|5|Briefly described|p11, p21|||Of Large and Wilson (1987) - included in Owen Group, based on litholological similarities. Basal, locally-derived conglomerate+sandstone (up to 150m thick) overlain by black (pyritic) to grey shale+siltstone with some micaceous sandstone, also ~150m thick||||||07-FEB-11
19660|Wedge River Beds|30277|6|Mentioned|p207|||Map on p207. Precambrian age. Refers Corbett(1970 unpubl.)||||||10-OCT-07
19660|Wedge River Beds|37933|3|Fully described|p553|||See also Fig.1.||||||
19660|Wedge River Beds|38157|6|Mentioned|p287|||||||||
19660|Wedge River Beds|41694|6|Mentioned|Map legend|Late Precambrian||||||||
19660|Wedge River Beds|42227|3|Fully described|p19|||||||||
19660|Wedge River Beds|68243|6|Mentioned|p649, p654, p655, p656|Neoproterozoic|Neoproterozoic|Corbett (1970). Approximately 300m thick.||||Unconformably overlain by the Island Road Formation. |Comprises a deformed conglomeratic succession.|
19660|Wedge River Beds|69859|5|Briefly described|Map legend|Neoproterozoic|Mesoproterozoic|Tyennan region.|||||Schistose conglomerate, quartzite, slate, phyllite and silicified carbonate: sequences of uncertain assignment.|06-AUG-15
19660|Wedge River Beds|73320|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Tyennan and similar regions. Map unit of schistose conglomerate, quartzite, slate, phyllite and silicified carbonate includes Wedge River Beds and sequences of uncertain assignment. Overlies inferred angular unconformity. Uncertainty between Mesoproterozoic and Neoproterozoic age indicated.||||||
19767|Wescott Dolomite Beds|41795|6|Mentioned|p49|||||||||
29133|West Coast Lamprophyres|33354|6|Mentioned|p186|||Age: between Middle Devonian and Late Mesozoic. The youngest rocks intruded by these lamprophyres are Middle Devonian, but the lamprophyres may be equivalent to similar rocks on King Island dated as late Mesozoic.||||||04-MAY-22
19782|West Coast Range Conglomerate|30277|6|Mentioned|p212|||Refers Hills and Carey(1929).||||||10-OCT-07
19782|West Coast Range Conglomerate|41795|6|Mentioned|p47|||||||||
19782|West Coast Range Conglomerate|69871|6|Mentioned|p3 Fig.1.2|||||||||
19782|West Coast Range Conglomerate|69874|6|Mentioned|p213|||Nye et al. (1934), Connelly (1947); later the Owen Conglomerate (Wade and Solomon, 1958) then Owen Group (Corbett, 1990).||||||
19781|West Coast Range Conglomerate Series""|30277|6|Mentioned|p211|||Refers Nyd(1927).||||||10-OCT-07
75542|West Coast Range Conglomerates|24601|6|Mentioned|p839|||Superseded name for the Owen Conglomerate; given by Connolly (1947).||||||30-NOV-09
31332|West Coast granite|24197|5|Briefly described|p107|||Informal name. Proterozoic granites in the western and northern parts of King Island. Adamellite to granodiorite, predominantly fine- to medium-grained with minor phases of porphyritic granite. Referred to as "West Coast granites" by Gresham (1972).||||||07-FEB-11
31332|West Coast granite|69873|6|Mentioned|p62|||Gresham (1972). An informal name superseded by its components: Loorana and Cape Wickham Granites.||||||
74102|West Coast granite""|24197|6|Mentioned|p107|||Informal name of Gresham (1972) for Proterozoic granites in the western and northern parts of King Island. Adamellite to granodiorite, predominantly fine- to medium-grained with minor phases of porphyritic granite.||||||07-FEB-11
74103|West Coast granites|24197|6|Mentioned|p107|Neoproterozoic|Neoproterozoic|Informal name for granites of the west coast of King Island. See also "West Coast granite" (Gresham 1972) and West Coast granite. Ages: 715Ma (McDougall and Leggo 1965), 767+/-10Ma (Black 1993) and 763+/-12Ma and 748+/-2Ma (Cox 1993).||||||07-FEB-11
74076|West Tamar Highway Basalt|61395|5|Briefly described|p29, p31 Tb. 3.1|||This is the 'keratophyre' of Green (1959) and an informal name. See also West Tamar Highway basalt and the reference to West Tamar Highway quartzwacke sandstones and siltstones - all are names for part(s) of Blyths Creek Fm.||||||07-FEB-11
74076|West Tamar Highway Basalt|69874|6|Mentioned|p180|||Beaconsfield area. Geochemistry described in some detail.||||||
19794|West conglomerate""|31472|6|Mentioned|Table 1|||||||||
73304|Westcott Formation|638|5|Briefly described|p100|||Together with Salisbury Formation, overlies the Natone Volcanics. Together these comprise a sequence of green dolomitic siltstone with interbedded greywacke and lenses of polymict conglomerate. ||||||
73304|Westcott Formation|63238|6|Mentioned|p11|||||||||
73269|Westcott dolomitic beds|63240|5|Briefly described|p4|||Redesignated from "Rosebery Group" to marine Owen Group from fossil evidence and lithology, together with Stitt Quartzite, Munro Slate and Quartzite, Salisbury fuchsitic conglomerate and Natone Volcanics.||||||10-DEC-07
40419|Western Ahrberg Group|24604|5|Briefly described|p907 Fig. 4|Neoproterozoic|Neoproterozoic|Informal - see the Ahrberg Group.||||||
25614|Western Formation|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Possibly misspelt? Should be Weston Formation of the Woodbridge Group.  Bryozoan mudstone.||||||07-FEB-08
73811|Western Volcano-Sedimentary Sequence""|638|5|Briefly described|p89-91 Figs. 4.3 and 4.4|||Informal term for sequence which includes volcano-sedimentary and sedimentary sequences, Miners Ridge Sandstone and basaltic-andesite volcanics. Also known as the "Western Sequence" section of Mount Read Volcs. Unconf.contact with Central Volcanic Complex||||||
79514|Western Volcano-Sedimentary Sequences|69874|4|Described|p150-153, p155, p158-165, p171, p176|Drumian|Drumian|See also p180-181. Dundas-Fossey Trough, western margin. Fossey Mountains area; underlies correlates of Tyndall Group. Lower part interfingers with north end of Kershaw Pumice Formation. Appears also as Western Volcano-Sedimentary Sequence, sequence, sequences; usually abbreviated in the text to WVSS. Hosts many andesitic to basaltic volcanic centres and intrusive bodies, [eg Que-Hellyer Volcanics] that tend to concentrate in younger part of pre-Tyndall sequence and Tyndall Group itself, eg Lynch Creek Basalt.||Mount Read Volcanics|Includes Mount Charter Group, White Spur Formation, Yolande River Sequence.|Intruded by Lynch Creek Basalt. Contacts Central Volcanic Complex. Underlies Tyndall Group (correlates), Blyths Creek Formation.|10-30km wide belt of volcanic-rich sequence; turbidites, mass-flows, siltstones, mudstones, conglomerates, andesitic-basaltic lavas & breccias.|
73122|Western Volcano-Sedimentary Sequences""|44135|5|Briefly described|p16|||Informal assoc. in Mt Read Volcanics. Extensive successions: interbedded tuffaceous sst., siltst., shale + volcaniclastic mass-flow conglomerate+breccia incl: Yolande River and Henry Fault Wedge Seqs., White Spur Fm., part of Dundas Gp and Mt Charter Gp.||||||07-DEC-09
83428|Western Volcano-sedimentary Sequence|69842|5|Briefly described|p3, 4-11|||Castra map; correlated with Cambrian sequence in Castra area. Ulverstone map; contact with Barrington Chert is highly speculative (?flat-lying thrust). Latrobe, Railton maps: correlation with Bott Conglomerate.||Mount Read Volcanics.||Correlated with Bott Conglomerate.||
37234|Western"" Ahrberg Group|23990|6|Mentioned|p168 Fig.1|||Informal name.||||||
19829|Westfield Beds|13995|5|Briefly described|p73, p76|Ordovician|Ordovician|Mole Creek-Florentine Valley area. Contains Eastonian bryozoans (listed) with close similarities with those in the Cincinnati area (USA). See also references to Westfield Sandstone (p74, p85, p109).||||Overlies Benjamin Limestone.||
19829|Westfield Beds|23187|6|Mentioned|p236||Bolindian|||||||
19829|Westfield Beds|29608|6|Mentioned|p46|||||||||
19829|Westfield Beds|30277|2|Defined|p226|Late Ordovician|Late Ordovician|||||||
19829|Westfield Beds|30279|6|Mentioned|p125|||Part of Gordon Subgroup.||||||01-MAY-08
19829|Westfield Beds|33738|6|Mentioned|p58|||||||||
19829|Westfield Beds|35118|6|Mentioned|p429|||||||||
19829|Westfield Beds|35671|4|Described|p5|||Discussion re definition of this unit.||||||
19829|Westfield Beds|35853|6|Mentioned|Fig.1|||Stratigraphic column showing range of conodontophorids.||||||
19829|Westfield Beds|36047|5|Briefly described|p365|||||||||
19829|Westfield Beds|36122|6|Mentioned|Fig.1|||||||||
19829|Westfield Beds|37756|6|Mentioned|p70|||||||||
19829|Westfield Beds|39235|6|Mentioned|Map legend|Silurian|Silurian|Probably  Silurian.||||||01-MAY-08
19829|Westfield Beds|40708|5|Briefly described|p95|||||||||
19829|Westfield Beds|40727|6|Mentioned|Fig.5|||||||||
19829|Westfield Beds|42478|6|Mentioned|p3, p7|||Used 1975. Superseded by Arndell Sandstone 1979 and Westfield Sandstone 1991.||||||01-MAY-08
19829|Westfield Beds|45118|6|Mentioned|p3|||[Originally entered for NSW. CEBMar95]||||||
19828|Westfield Beds""|41793|6|Mentioned|p56|||||||||
29134|Westfield Formation|41954|6|Mentioned|Table 1 P12|||||||||
19830|Westfield Sandstone|13995|5|Briefly described|p74, p85, p109|Late Ordovician|Late Ordovician|Appears as Westfield (=Arndell) Sandstone, suggesting the former superseded the latter name. The lower beds had been dated as basal Silurian age; may in fact be Hirnantian (latest Ordovician). Contains a new trinucleid trilobite: biogeographic links. See also references to Westfield Beds (p73, p76).||||||
19830|Westfield Sandstone|13996|6|Mentioned|p139, p143|||Llandovery-aged brachiopod assemblages described. Hosts an undescribed trilobite fauna of probable Rhuddanian age.||||||
19830|Westfield Sandstone|23187|5|Briefly described|Fig2p237||Bolindian|||||||
19830|Westfield Sandstone|40126|6|Mentioned|p14|||||||||
19830|Westfield Sandstone|40127|6|Mentioned|p11|||||||||
19830|Westfield Sandstone|40136|5|Briefly described|p43|||||||||
19830|Westfield Sandstone|41954|6|Mentioned|p11|||||||||
19830|Westfield Sandstone|42478|1|Redefined|p7|||Formerly  Arndell Sandstone of Baillie (1979) and Westfield Beds of Corbett & Banks (1974).||||||10-OCT-07
19830|Westfield Sandstone|63170|6|Mentioned|p201||Silurian|Equivalent to Arndell Sandstone.||||||07-FEB-11
19830|Westfield Sandstone|69875|6|Mentioned|p244, p256|Early Silurian|Ordovician|Of Laurie (1991) = Arndell Sandstone (Baillie, 1979).||||||18-SEP-17
74386|Westfield beds|63170|6|Mentioned|p201|||Of Corbett and Banks (1975). Included in the redefined Gordon Subgroup (Corbett and Banks 1974).||||||07-FEB-11
74386|Westfield beds|69875|6|Mentioned|p244|Early Silurian|Ordovician|Corbett and Banks (1975); Baillie (1979) [both of whom actually used Westfield Beds]. Subsequently Arndell Sandstone (Baillie, 1979).||||||18-SEP-17
26997|Weston Formation|24549|4|Described|p7|Permian|Permian|Of the Woodbridge Group. Max Thickness: 40ft. Dark grey micaceous mudstone with rich bryozoan fauna and occasional brachiopods||||||10-OCT-07
26997|Weston Formation|31195|6|Mentioned|Map legend|Permian|Permian|||||||
26997|Weston Formation|32627|6|Mentioned|p29|Permian|Permian|Informally named in the Dabool-Weston-Garcia Formations grouping in stating that these units have "generally not been separated during mapping".||||||07-FEB-08
26997|Weston Formation|43474|14|Not recorded|p11|||||||||
26997|Weston Formation|63172|5|Briefly described|p308 Fig. 10|||||||||07-FEB-11
26997|Weston Formation|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
78600|Wet Beds|61395|6|Mentioned|p60|Ordovician|Ordovician|So named because of the amount of water entering the mine when this unit was intersected. see also Fig 5.1. Equivalent to upper section of Salisbury Hill Formation.||Unit in Lower Transition Beds|||Interbedded granule-pebble conglomerate, granule conglomeratic sandstone, and dark grey fine and medium sandstone.|16-JAN-14
79586|Wet Beds Conglomerate|69876|5|Briefly described|p342-344|Ordovician|Ordovician|Apparently synonymous with Wet Beds Member. [Needs to have the rank of Member].Beaconsfield Gold Mine informal stratigraphy. Name from unpublished sources.||Salisbury Hill Formation||Underlies Eaglehawk Gully Formation [Pebble Beds Member] conformably.|Granule conglomerate, granule conglomeratic sandstone and fine and medium grained sandstone.|16-JAN-17
79587|Wet Beds Member|69876|5|Briefly described|p343|Ordovician|Ordovician|Apparently synonymous with Wet Beds Conglomerate.Beaconsfield Gold Mine informal stratigraphy. Name from unpublished sources.||Salisbury Hill Formation||||16-JAN-17
74916|Wet Beds""|64396|5|Briefly described|p210 Fig. 2, p211|Ordovician|Ordovician|Historical term for the Lower Transition Beds; the Transition Beds are the host rocks for the mineralisation in the Beaconsfield Goldfield.||||||08-DEC-08
74387|Wherrets Chert Member|63170|5|Briefly described|p202|||Upper section of Karmberg Limestone. Thickness: 180m. Consists of micrite with chert beds near its base and chert nodules higher up.||||||07-FEB-11
74388|Wherrets Member|63170|6|Mentioned|p202|||Abbreviated version of Wherrets Chert Member (Karmberg Limestone).||||||07-FEB-11
81520|White Heemskirk Granite|71100|5|Briefly described|p126-127,129-130,132-135|Famennian|Famennian|S-type strongly peraluminous granite. Also referred to as Heemskirk White on p126. Of the Heemskirk Granite, red phase defined by consistent K-feldpsar (white K-spar) colour differences. LA-ICP-MS zircon U-Pb dating yields concordia intercept age of 364.1+\-6.7/7.3 Ma, within analytical error of 361+\-2 Ma of Black et al., 2005. Rb-Sr whole rock age of 350+\-6 Ma (Brooks and Compston, 1965).|361+\-2 Ma||||Fine- to coarse-grained, equigranular, locally porphyritic. Quartz, K-feldspar, plagioclase, and minor biotite, trace zircon, monazite, titanite, magnetite/ilmenite, apatite, fluorite, muscovite, garnet and cassiterite.|
19904|White Quartzite Stage""|42358|5|Briefly described|p11|||Used 1934. Now part Cowrie Siltstone correlate.||||||
19911|White Schist""|41815|6|Mentioned|Map legend|Precambrian||||||||
73287|White Spur Formation, Lower|63238|5|Briefly described|p20 Fig. 3|Middle Cambrian|Middle Cambrian|Informal - see White Spur Formation. ||||||
73286|White Spur Formation, Upper|63238|6|Mentioned|p19 Fig. 2|||Informal - see White Spur Formation. ||||||
29416|Whitehorse Beach Sandstone|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
29416|Whitehorse Beach Sandstone|42958|5|Briefly described|p48|||of Spero Bay Group. Misspelling of Whitehorses Beach Sandstone.||||||
29416|Whitehorse Beach Sandstone|63170|5|Briefly described|p225 Fig. 6.12, p229|Emsian|Emsian|Of Spero Bay Group. Overlies Red Reef Cliff Sandstone. Thickness: 60m. In the Western Tasmania Terrane. Well-sorted, cross-bedded quarts-sandstone with minor siltstone and conglomerate.||||||07-FEB-11
29416|Whitehorse Beach Sandstone|65214|6|Mentioned|p273|Devonian|Devonian|TAS, Point Hibbs, TAS. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
81866|Whyte Pine Granite|69050|6|Mentioned|p40|||Of Camacho (1987).||||||06-MAY-20
73434|Whyte River Complex""|63168|6|Mentioned|p66|||Informal - see Whyte River Complex.||||||
19955|Whyte River Schist|45087|5|Briefly described|p225|||Chemical analyses.||||||10-OCT-07
29140|Whyte Schists|33839|6|Mentioned|p567|||||||||
29140|Whyte Schists|38638|6|Mentioned|Fig.2|||||||||
29140|Whyte Schists|39475|6|Mentioned|Fig.1|||||||||
19957|Whyte schists|38638|6|Mentioned|p1901|||||||||
19957|Whyte schists|39475|6|Mentioned|Fig.1|||||||||
69916|Wickham schist|61263|5|Briefly described|p463 Fig. 2|Neoproterozoic|Neoproterozoic|Age: 769+/-25Ma. On King Island. Of the Wickham Orogeny.||||||
73437|Wilson River Complex|63168|6|Mentioned|p71|||Also referred to as the Wilson River Ultramafic Complex.||||||
73437|Wilson River Complex|63169|5|Briefly described|p158|||Refers to Wilson River Ultramafic Complex. Includes layered pyroxenite-dunite and layered dunite-harzburgite ultramafic associations.Geological Province: Dundas Trough.||||||31-OCT-07
20167|Wilson River complex|41594|6|Mentioned|p27|||||||||
20167|Wilson River complex|42838|5|Briefly described|p374|||||||||
20167|Wilson River complex|43191|6|Mentioned|p46|||Contains ultramafic associations.||||||10-OCT-07
20170|Wilsonia Volcanics""|31475|6|Mentioned|p85|||||||||
30097|Windmill Hill Beds|43088|5|Briefly described|p29|||||||||
34214|Wings Quartzite|22668|6|Mentioned|p27|||||||||
34214|Wings Quartzite|69859|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Adamsfield-Jubilee region.|||||Massive quartz sandstone.|
34214|Wings Quartzite|73320|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Adamsfield - Jubilee region. Underlies low-angle unconformity or inferred discontinuity. Uncertainty between Mesoproterozoic and Neoproterozoic age indicated.|||||Massive quartz sandstone.|
81371|Winterbrook felsic volcanic|70274|6|Mentioned|p450|Cambrian|Cambrian|Intrusion within the Tyndall Group, with U-Pb SHRIMP zircon age of 500.4+\-13.8 Ma.|500.4+\-13.8 Ma|||||
73435|Within Plate Basalt|63168|5|Briefly described|p47, p64, p68|||Abbreviated version of  Within Plate Tholeiite-Alkaline Basalt. Not intended as a formal name - indicates a type of basalt as does Ocean Floor Basalt. Names used interchangeably in text. ||||||
73436|Within Plate Tholeiite-Alkaline Basalt|63168|6|Mentioned|p47|||See also Within Plate Basalt. Names used interchangeably.||||||
33458|Wombat Flat Adamellite|44105|4|Described|p254|||Part of Meredith Batholith.||||||10-OCT-07
20482|Woodbridge Formation|24548|3|Fully described|p8|Permian|Permian|Overlying Unit: Ferntree Mudstone (conformable). Underlying Unit: Liffey Sandstone (conformable). Max Thickness: 335ft. Contains a richly fossiliferous bed 50ft from the top of the formation||||||
20482|Woodbridge Formation|30889|6|Mentioned|p46|||||||||
20482|Woodbridge Formation|34098|6|Mentioned|p133|||Perm.  See also PP134,137||||||
20482|Woodbridge Formation|38505|6|Mentioned|p1118|||||||||
20483|Woodbridge Glacial Formation|24548|5|Briefly described|p7 Fig.III|Permian|Permian|Informal name - see Woodbridge Formation. See also Golden Valley Map 4687||||||
20483|Woodbridge Glacial Formation|31706|6|Mentioned|p671|||Correlation chart of Gondwana System||||||
20483|Woodbridge Glacial Formation|33494|6|Mentioned|p45|||||||||
20483|Woodbridge Glacial Formation|34047|6|Mentioned|p83|||Perm.||||||
20483|Woodbridge Glacial Formation|34099|6|Mentioned|Fig.1|||||||||
20483|Woodbridge Glacial Formation|41895|5|Briefly described|p11|||Redefined and renamed Truro Tillite in Kingsborough area, Malbina Formation in Hobart area||||||
25646|Woodbridge Glacial Formation""|42320|6|Mentioned|p10|||Old name for Malbina Formation rocks.||||||
20484|Woodbridge Glacials|36788|6|Mentioned|Fig.4|||||||||
20484|Woodbridge Glacials|63820|5|Briefly described|Map legend|Permian|Permian|||||||
20486|Woodbridge Group|24549|4|Described|p7|Permian|Permian|Max Thickness: 270ft. Sandstones and mudstones and occasional bands of limestone.||||||06-FEB-08
20486|Woodbridge Group|34047|6|Mentioned|p83|Permian|Permian|See also p84. Permian.||||||06-FEB-08
20486|Woodbridge Group|34316|5|Briefly described|p21 Fig.3|Late Permian|Late Permian|Includes Meander, Dabool and Western Formations.||||||06-FEB-08
20486|Woodbridge Group|36788|6|Mentioned|Fig.4|||||||||
20486|Woodbridge Group|36799|4|Described|p11|||||||||
20486|Woodbridge Group|41895|6|Mentioned|p11|||Replaced by Poatina Group in Central Plateau area in 1969.||||||06-FEB-08
20486|Woodbridge Group|63263|5|Briefly described|p33 Fig. 7|||||||||07-FEB-11
20486|Woodbridge Group|67543|5|Briefly described|p145 Fig.4|||Fig.4 suggests correlation with West Arm Group and Deep Bay Formation.|||||Fossiliferous siltstone and fine sandstone.|
20485|Woodbridge Group""|23837|6|Mentioned|p440 Fig.2|||||||||
20485|Woodbridge Group""|36788|6|Mentioned|p29|||||||||
20485|Woodbridge Group""|36817|6|Mentioned|p62|||||||||
20487|Woodbridge Series|34047|6|Mentioned|p83|||Perm.||||||
20488|Woodbridge Tillite|30155|5|Briefly described|p455|||||||||
20488|Woodbridge Tillite|30156|6|Mentioned|p37|||At least 275m thick at Cygnet, absent at Hobart.||||||
20489|Woodbridge Tillitic Mudstone|45042|6|Mentioned|p34|||Permian. See P35, Plate 1||||||
31097|Woodbridge formation|43477|14|Not recorded|p45||Permian|Correlated with Maitland Group in NSW. Ref. to Brill 1956||||||
31931|Woodbridge glacial formation|43876|6|Mentioned|p587||Permian|See also Lexicon||||||
20490|Woodbridge"" Formation|34099|6|Mentioned|p11|||||||||
20491|Woodbridge"" Group|34099|6|Mentioned|p11|||||||||
20525|Woodridge Group|34098|6|Mentioned|p137|||Perm.||||||
79582|Woodstock Surface|69879|5|Briefly described|p444-445|Miocene|Miocene|Woodstock Surface (Nicolls 1960). Regolith. Lateritisation of the Woodstock Surface may have coincided with the mid-Miocene Climatic Optimum.|15-17 Ma.||||Widespread remnants of an extensive landscape surface marked by laterite or lag pisolithic iron oxide. Laterised tholeiites include significant bauxite deposits. Developed on post-basalt deposits of weakly-cemented siliceous gravel.|
20533|Woody Island Formation|24552|4|Described|p5 Fig.2, p6|Asselian|Asselian|Poorly fossiliferous massive bedded pyritc, carbonaceous, glendonitic mudstone and siltstone. Conformably overlies Truro Tillite. Conformably overlain by Bundella Mudstone. Of the Lower Parmeener Supergroup. Geological Province: Tasmanian Basin.||||||07-FEB-11
20533|Woody Island Formation|30150|6|Mentioned|Fig.5|||||||||
20533|Woody Island Formation|36020|6|Mentioned|p388|||||||||
20533|Woody Island Formation|39579|6|Mentioned|p13|||||||||
20533|Woody Island Formation|41895|5|Briefly described|p11|||FD as Woody Island Siltstone (p15).||||||10-OCT-07
20533|Woody Island Formation|42000|6|Mentioned|p53|||||||||
20533|Woody Island Formation|43021|5|Briefly described|Fig.2,p462|||||||||
20533|Woody Island Formation|43022|6|Mentioned|p472|||||||||
20533|Woody Island Formation|49644|5|Briefly described|Table|||||||||
20533|Woody Island Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Beckers Formation, Lochinvar Formation, Wasp Head Formation and Quamby Formation. Geological Province: Tasmanian Basin||||||
20533|Woody Island Formation|63172|5|Briefly described|p296 Fig. 8.1|Early Permian|Late Carboniferous|Informal - see Woody Island Siltstone. Overlain by Bundella Formation; overlies Truro Formation. See also p304 Fig. 8.7.||||||07-FEB-11
20533|Woody Island Formation|63263|6|Mentioned|p38, p45|Early Permian||Misnamed and should be Woody Island Siltstone. Consists of monotonous, dark grey, thick-bedded to massive pyritic siltstone or mudstone generally lacking in fossils; includes tasmanite beds. See also  p33 Fig. 7.||||||07-FEB-11
20533|Woody Island Formation|65645|6|Mentioned|p17|Permian|Carboniferous|Adjacent to gold bearing quartz syenite.||||||
20533|Woody Island Formation|67543|5|Briefly described|p144 Fig 3, p145 Fig.4|Sakmarian|Sakmarian|Fig.4 suggests correlation with Quamby and Inglis Formations.||Of the Parmeener Supergroup.||Overlies Wynyard Formation or Truro Tillite. Is overlain by Bundella Formation.||13-OCT-17
20533|Woody Island Formation|69877|4|Described|p364 Fig.7.1, p366-368, p372, p382|Asselian|Carboniferous|Poorly fossiliferous. Correlation and fossil age range chart. Potential source rock for hydrocarbons: contains type III gas and oil prone kerogens.||Unit in Lower Parmeener Supergroup.|Includes Tasmanite Oil Shale.|Overlies Wynyard and Truro Tillites. Is overlain by Bundella Formation. Correlative with Quamby Formation.|Dark, organic, poorly sorted, fine- to medium-grained siltstone; contains dropstones, glendonites, rare marine fossils; lightly bioturbated.|
20533|Woody Island Formation|69879|6|Mentioned|p454 Fig9.37|Permian|Permian|||||Intruded by Jurassic dolerite, Cygnet Alkaline Complex.||
20533|Woody Island Formation|70194|6|Mentioned|p297, p299|Early Permian|Late Carboniferous|||Of Parmeener Supergroup.|Includes Tasmanite Oil Shale.|Laterally equivalent to Quamby Formation. Underlain in part by Wynyard - Truro Formations, and unconformably by Mathinna Group.|Includes black shale.|
20533|Woody Island Formation|73639|6|Mentioned|p3 Fig.2|Permian|Permian|See also reference to Woody Island Siltstone (p3).||Lower Parmeener Supergroup||||
20534|Woody Island Siltstone Formation|30819|6|Mentioned|p107|||||||||
20674|Wurawina Supergroup""|40708|4|Described|p95|||||||||
73123|Wurawina Supergroup, lower|44135|6|Mentioned|p24|||Informal - see Wurawina Supergroup.||||||07-DEC-09
74079|Wurawira Supergroup|61395|5|Briefly described|p2 Fig. 1.1|Early Devonian|Late Cambrian|Non-marine siliciclastic conglomerate and marine shelf sequences. In western Tasmania.||||||07-FEB-11
20675|Wuriwina Supergroup|41908|6|Mentioned|p44 Fig.1|||Misspelling of Wurawina?||||||
20705|Wybalenna Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
20705|Wybalenna Granite|61216|5|Briefly described|p19 Fig. 7|Early Devonian|Early Devonian|Presented as Wybalenna only in map of granites. Age: 400.5+/-4.0Ma.||||||10-FEB-11
20705|Wybalenna Granite|63540|5|Briefly described|Map legend|Devonian|Devonian|Of the Wybalenna Suite. I-type, felsic granite; weakly to moderately fractionated, reduced. Name implied from map legend.||||||25-SEP-07
20705|Wybalenna Granite|66575|5|Briefly described|p935 Fig1, p943 Fig6, p951 Tb.2,|Emsian|Emsian|U-Pb SHRIMP age of 401 +/- 4 Ma; I-Type; mafic, unfractionated. Inherited zircons discussed.||||||
20705|Wybalenna Granite|69876|5|Briefly described|p304, p306 Tb 6.1, p308, p311|Middle Devonian|Early Devonian|Furneaux Group. Geochemistry.|c.405-396 Ma (SHRIMP U-Pb).|Wybalenna Suite|||I-type.|
37067|Wynward Tillite|23718|4|Described|p27|Carboniferous|Carboniferous|||||||
81144|Wynyard - Truro Formations|70194|6|Mentioned|p299 Fig 2|Gzhelian|Moscovian|||Of Parmeener Supergroup.||Overlain by Quamby Formation and Woody Island Formation. Underlain unconformably by Eldon Group.||
20721|Wynyard Formation|37926|6|Mentioned|p495|||||||||
20721|Wynyard Formation|43021|6|Mentioned|p459|||||||||
20721|Wynyard Formation|63172|5|Briefly described|p296 Fig. 8.1|Late Carboniferous|Late Carboniferous|Informal - see Wynyard Tillite.||||||07-FEB-11
20721|Wynyard Formation|63263|5|Briefly described|p33 Fig. 7|||Misspelt - should be Wynyard Tillite.||||||07-FEB-11
20721|Wynyard Formation|67543|4|Described|p142-154|Sakmarian|Gzhelian|Deposited in a proglacial environment; the depositing glacier(s) occupied a ~40km wide trough in NW Tasmania. Records ice rafting, gravity flows, glacial outwash, and suspension settling and dewatering. ~ 600m thick. Fig.4 suggests correlation with Truro Tillite and Stockers Tillite. Appears also as Wynyard "Tillite" in Fig.5.||Of the Parmeener Supergroup.||Overlain by the Inglis Formation or Woody Island Formation.|Four facies associations: massive diamictite, stratified diamictite, conglomerate and sandstone, deformed mudstone and fine sandstone.|
20723|Wynyard Tillite Formation|30819|6|Mentioned|p107|||||||||
78475|Yarrow Creek Siltstone|67493|6|Mentioned|p15, p32, p56  |||Unexplained mis-naming of Yarrow Creek Mudstone on 3 occasions in this article.||||||
31359|Yolande River sequence|22551|6|Mentioned|p151 Fig.3|||||||||
31359|Yolande River sequence|22627|5|Briefly described|fig4p129, p130|Late Cambrian|Middle Cambrian|||||||
31359|Yolande River sequence|43131|4|Described|p570|Cambrian|Cambrian|Informal unit of Mount Read Volcanics.||||||
31359|Yolande River sequence|69876|6|Mentioned|p288|Cambrian|Cambrian|Strahan-Queenstown area. Gravity modelling.||||||
21081|Zeehan Conglomerate|22627|6|Mentioned|p132|Cambrian|Cambrian|||||||
21081|Zeehan Conglomerate|41795|6|Mentioned|p45|||||||||
21082|Zeehan Glacials""|31468|6|Mentioned|p13|||||||||
21083|Zeehan Tillite Formation|37926|6|Mentioned|p495|||||||||
40416|eastern"" Ahrberg Group|24604|5|Briefly described|p903|Neoproterozoic|Neoproterozoic|Informal - see the Ahrberg Group||||||
35878|metamorphic rock 35878|35828|6|Mentioned|Map legend|Precambrian|Precambrian|Metamorphic rocks. Pelitic sequences.||||||
40420|western"" Ahrberg Group|24604|5|Briefly described|p903|Neoproterozoic|Neoproterozoic|Informal - see the Ahrberg Group.||||||
