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
21100|Adder Dacite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
21100|Adder Dacite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
21100|Adder Dacite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
21100|Adder Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V129. I-Type.||||||
21100|Adder Dacite|23616|5|Briefly described|Table 3 p49|||Of Boonmoo Volcanic Subgroup||||||
21100|Adder Dacite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).  Hornblende dacitic to rhyolititic ignimbrite, strongly porphyritic; pumice 'flamme'.||||||15-JUN-06
21100|Adder Dacite|43259|4|Described|Appendix 1,p14.||Late Carboniferous|Of Boonmoo Volcanic Subgroup.||||||03-JUN-09
21100|Adder Dacite|43567|5|Briefly described|Table 2,p400|||||||||
21100|Adder Dacite|43626|2|Defined|p26||Late Carboniferous|Between 306+/-3 Ma and 304+/-4 Ma.||||||03-JUN-09
21100|Adder Dacite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21100|Adder Dacite|60425|5|Briefly described|p48 Tb. 3|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21100|Adder Dacite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A "geophysical subdivision" of this unit, described as a probable variant, is mapped separately.||Unit in Boonmoo Volcanic Subgroup.|||Dark to greenish or purplish grey, lithics-poor to moderately lithics-rich, moderately to very crystal-rich, hornblende-biotite dacitic to rhyodacitic ignimbrite.|
21115|Allsorts Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Tennyson Volcanic Subgroup of Featherbed Volcanic Group.||||||
21115|Allsorts Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Tennyson Volcanic Subgroup.||||||
21115|Allsorts Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V124. I-Type.||||||
21115|Allsorts Rhyolite|23616|5|Briefly described|Table 3 p48||Late Carboniferous|Of Tennyson Volcanic Subgroup.||||||
21115|Allsorts Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Tennyson Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21115|Allsorts Rhyolite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|Of Kooboora Volcanic Subgroup.||||||03-JUN-09
21115|Allsorts Rhyolite|43626|2|Defined|p31|Early Permian|Late Carboniferous|Between 289+/-7 Ma and 306+/-3 Ma.||||||03-JUN-09
21115|Allsorts Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21115|Allsorts Rhyolite|60425|5|Briefly described|p46 Tb. 3|Late Carboniferous|Late Carboniferous|Of Tennyson Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21115|Allsorts Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Four facies associations are mapped separately.||Unit in Tennyson Volcanic Subgroup.|||Poorly welded, crystal-poor, rhyolitic ignimbrite, flow-banded, slightly porphyritic rhyolitic lava; vitric tuff, volcanic sandstone to siltstone, unwelded rhyolitic ignimbrite;  andesite; rhyolitic ignimbrite, volcanic sandstone, vitric tuff.|
21117|Almac Granodiorite|23291|5|Briefly described|p44|Late Carboniferous|Late Carboniferous|Intrudes the Pratt Volcanics. Of the Almaden Supersuite. Geological Province: Georgetown Region.||||||08-JUL-15
21117|Almac Granodiorite|23423|5|Briefly described|p235||Late Carboniferous|Almaden Supersuite||||||
21117|Almac Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 301. I-Type.||||||
21117|Almac Granodiorite|23713|5|Briefly described|p74 Appendix 2|||Intrudes Dargalong Metamorphics, Chillagoe Formation and Pratt Volcanics. Of Almaden Supersuite. Overlying unit Gilbert River Formation - unconformable.||||||
21117|Almac Granodiorite|24485|6|Mentioned|p40|||||||||
21117|Almac Granodiorite|43083|4|Described|p252|||Of Almaden Supersuite. I-type.  Lithology included.||||||17-JUN-09
21117|Almac Granodiorite|43087|6|Mentioned|p91|||||||||
21117|Almac Granodiorite|43254|5|Briefly described|map legend||Late Carboniferous|of Almaden Supersuite.||||||
21117|Almac Granodiorite|43259|4|Described|Appendix 1,p37.||Late Carboniferous|||||||
21117|Almac Granodiorite|43625|6|Mentioned|p34|||Age: 300-310 Ma||||||
21117|Almac Granodiorite|60425|4|Described|p51 Tb. 3, p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Cuts into Pratt Volcanics. I-type. Fine-gr., mod'l to highly porphyritic (augite-) biotite-hornblende granodiorite to quartz monzodiorite or quartz monzonite; more lithology included. See also p60 Tb. 4.||||||07-FEB-11
21120|Alpha Granite|23049|3|Fully described|p56|Devonian|Silurian|Age: 394+/-30Ma.||||||
21120|Alpha Granite|23283|2|Defined|p24|Devonian|Silurian|||||||
21120|Alpha Granite|23505|5|Briefly described|Map legend|Devonian|Silurian|Of Amarra Supersuite.||||||24-JUL-08
21125|Amarra Granite|23049|3|Fully described|p19|Early Devonian|Early Devonian|Age: 382+/-5Ma. of Amarra Suite.||||||
21125|Amarra Granite|23283|2|Defined|p19|Devonian|Silurian|||||||
21125|Amarra Granite|23422|5|Briefly described|p177, p216 Table 6.10|Middle Devonian|Early Devonian|Of Amarra Supersuite.||||||
21125|Amarra Granite|23430|5|Briefly described|Table 14.2 p460.||Devonian|Zircon crystallisation 382 +/- 5 Ma. Lolworth Batholith Province||||||
21125|Amarra Granite|23505|5|Briefly described|Map legend|Devonian|Silurian|of Amarra Supersuite.||||||
21125|Amarra Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
21125|Amarra Granite|69592|5|Briefly described|p292-293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~800 km2.|382 +/- 5 Ma (SHRIMP U-Pb zircon: Fanning 1995).|Amarra Suite.|||Medium-grained, porphyritic, biotite and muscovite-biotite granite.|
21151|Aroonbeta Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Djungan Volcanic Subgroup of Featherbed Volcanic Group.||||||
21151|Aroonbeta Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21151|Aroonbeta Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Djungan Subgroup.||||||
21151|Aroonbeta Rhyolite|43259|6|Mentioned|Appendix 1,p11.||Early Permian|||||||
21151|Aroonbeta Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
21151|Aroonbeta Rhyolite|43626|2|Defined|p61||Early Permian|Age: between 281+/-2 Ma and 289+/-10 Ma.||||||03-JUN-09
21151|Aroonbeta Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Djungan Volcanic Group (Featherbed Volcanic Group). Geological Province: Kennedy Province. Pale grey, greenish grey, purplish brown, or brown, lithics-poor to lithics-rich, crystal-rich, rhyolitic ignimbrite; with mainly rhyolite clasts up to 20 cm.||||||
21151|Aroonbeta Rhyolite|60425|5|Briefly described|p46 Tb. 3|Early Permian|Early Permian|Of Djungan Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21151|Aroonbeta Rhyolite|62523|6|Mentioned|p6, p17|||Within the Djungan Cauldron. See also p16 Tb. 1.||||||07-FEB-11
21154|Arringunna Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Yongala Volcanic Subgroup of Featherbed Volcanic Group.||||||
21154|Arringunna Rhyolite|23430|5|Briefly described|p498|||Of Featherbed Volcanic Group||||||
21154|Arringunna Rhyolite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup. Age: 289+/-10Ma Rb-Sr.||||||
21154|Arringunna Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Age: 290+/-12 Ma, Rb-Sr. Of Yongala Volcanic Subgroup and Lags Supersuite.||||||
21154|Arringunna Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V109. A-Type.||||||
21154|Arringunna Rhyolite|23616|5|Briefly described|Table 3 p47||Permian|Rb-Sr total rock age 289+/-10 Ma. Of Yongala Volcanic Subgroup of Featherbed Volcanic Group.||||||
21154|Arringunna Rhyolite|23713|5|Briefly described|p22|||Age: 288+/-17 Ma, 290+/-12 Ma (Rb-Sr isotope). Underlying unit Combella Rhyolite||||||
21154|Arringunna Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group||||||
21154|Arringunna Rhyolite|43083|5|Briefly described|p92|||Age: 289+/-10 Ma (Rb-Sr). Of Featherbed Volcanic Group||||||17-JUN-09
21154|Arringunna Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup (Featherbed Volcanic Group).  Rhyolitic ignimbrite with pale, coarse porphyritic pumice clasts.  Age: 289+/-10Ma.||||||15-JUN-06
21154|Arringunna Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Yongala Volcanic Subgroup. Age 289+/-10 Ma.||||||
21154|Arringunna Rhyolite|43259|4|Described|Appendix 1,p11.||Early Permian|Of Yongala Volcanic Subgroup. Age is 289+/-10 Ma.||||||03-JUN-09
21154|Arringunna Rhyolite|43285|5|Briefly described|Map Legend||Permian|Of Featherbed Volcanic Subgroup.||||||03-JUN-09
21154|Arringunna Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
21154|Arringunna Rhyolite|43625|6|Mentioned|p38|||Age: 288+/-17 Ma, 290+/-12 Ma||||||
21154|Arringunna Rhyolite|43626|2|Defined|p54||Early Permian|Rb-Sr ages: 288+/-17 Ma and 290+/-12 Ma. may be intruded by Lags Micogranite (ring dyke).||||||21-AUG-15
21154|Arringunna Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
21154|Arringunna Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 289 +/- 10 Ma (Rb-Sr). Of Yongala Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
21154|Arringunna Rhyolite|60425|5|Briefly described|p45 Tb. 3, p46 Tb. 3|Early Permian|Early Permian|Of the Yongala Volcanic Subgroup (Featherbed Volcanic Group). Has two informal subunits. Age: 288+/-17Ma and 290+/-12Ma (Rb-Sr).||||||07-FEB-11
21154|Arringunna Rhyolite|62523|6|Mentioned|p19 Tb.2|||Within the Featherbed Cauldron.||||||07-FEB-11
21154|Arringunna Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province. Mapped separately, as is a geophysical subdivision described as a probable variant of the main unit.|291 +/- 12 Ma, 273 +/- 7 Ma (Rb-Sr, total rock).|Unit in Yongala Volcanic Subgroup.|||Dark bluish or greenish grey, very crystal-rich, rhyolitic ignimbrite with 'pumice' and rare rhyolite clasts and vitrophyre in places at/near base; locally with variably reacted garnet.|
21154|Arringunna Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Included in Lags Supersuite.|285 Ma.|Featherbed Volcanic Group.|||A-type.|
21170|Baby Granodiorite|23032|5|Briefly described|p39|||||||||
21170|Baby Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
21170|Baby Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
21170|Baby Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
21170|Baby Granodiorite|43480|2|Defined|7,14|Devonian|Silurian|||||||
21170|Baby Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Foliated pinkish-grey to greenish-grey, sparsely porphyritic muscovite-biotite, biotite-muscovite and garnet-biotite-muscovite granodiorite with plagioclase, biotite and quartz phenocrysts.|
21170|Baby Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Foliated pinkish-grey to greenish-grey, sparsely porphyritic muscovite-biotite, biotite-muscovite and garnet-biotite-muscovite granodiorite with plagioclase, biotite and quartz phenocrysts.|
21170|Baby Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
21188|Bamford Granite|23423|6|Mentioned|p306 Table 7.3|||||||||
21188|Bamford Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 303+/-5 Ma, Rb-Sr. of Ootann Supersuite.||||||
21188|Bamford Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 444. I-Type.||||||
21188|Bamford Granite|23616|6|Mentioned|Table 3 p48||Carboniferous|See also p99 Appendix 2.||||||
21188|Bamford Granite|43106|6|Mentioned|p30|||||||||
21188|Bamford Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).  Pale to medium grey or pink, medium to coarse biotite granite; variably greisenised. Age: 303+/-5Ma. .||||||23-APR-09
21188|Bamford Granite|43259|4|Described|Appendix 1,p48.||Late Carboniferous|Age is 303+/-5 Ma.||||||
21188|Bamford Granite|43567|5|Briefly described|Table 2,p401|||||||||
21188|Bamford Granite|43626|6|Mentioned|p11|||||||||
21188|Bamford Granite|60425|4|Described|p49 Tb.3, p184, p276-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Intruded Boonmoo Volcanic Subgroup. Age:303+/-5Ma(Rb-Sr). I-type. Grey, med.-to coarse-gr.biotite granite; variably/ locally extensively altered (greisenised) + patchy W-M0-Bi mineralisation (concentrated in pipes)||||||07-FEB-11
21188|Bamford Granite|67806|6|Mentioned|p114|||Has W-Mo-Bi mineralisation.||||||
21188|Bamford Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Other dating gives ages of 303 +/- 5 Ma (Rb-Sr, plagioclase), and 303 Ma (Rb-Sr, muscovite).|298 +/- 4 Ma (Rb-Sr, total rock).|Unit in Ootann Supersuite.|||Pale to medium grey, pinkish grey or pink, medium- to coarse-grained biotite granite; variably altered and mineralised.|
21211|Bedlog Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
21211|Bedlog Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
21211|Bedlog Rhyolite|23513|5|Briefly described|Map legend||Late Carboniferous|Palaeozoic Volcanic No. V92. I-Type.||||||
21211|Bedlog Rhyolite|23616|5|Briefly described|Table 3 p50||Carboniferous|Of Boonmoo Volcanic Subgroup||||||
21211|Bedlog Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21211|Bedlog Rhyolite|43259|4|Described|Appendix 1,p9.||Late Carboniferous|Of Boonmoo Volcanic Subgroup. Age is 313 Ma.||||||
21211|Bedlog Rhyolite|43567|5|Briefly described|Table 2,p401|||||||||
21211|Bedlog Rhyolite|43626|2|Defined|p18||Late Carboniferous|310-313 Ma||||||
21211|Bedlog Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21211|Bedlog Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21218|Belgravia Granodiorite|23423|5|Briefly described|p307 Table 7.3||Carboniferous|Intrudes Redcap Dacite.  See also p293.||||||
21218|Belgravia Granodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
21218|Belgravia Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 447. I-Type.||||||
21218|Belgravia Granodiorite|23616|6|Mentioned|Table 3 p51|||||||||
21218|Belgravia Granodiorite|24485|5|Briefly described|p44, p54 Tb.8|Late Carboniferous|Late Carboniferous|Intrudes the Redcap Dacite||||||
21218|Belgravia Granodiorite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
21218|Belgravia Granodiorite|43083|4|Described|p252|||Of Almaden Supersuite. I-type.  Lithology included.||||||17-JUN-09
21218|Belgravia Granodiorite|43087|2|Defined|p68|Late Carboniferous||||||||
21218|Belgravia Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).||||||15-JUN-06
21218|Belgravia Granodiorite|43259|4|Described|Appendix 1,p48.||Carboniferous|||||||
21218|Belgravia Granodiorite|43626|6|Mentioned|p98|||||||||
21218|Belgravia Granodiorite|60425|4|Described|p49 Tb.3, p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).Intruded Redcap Dacite. I-type. Med-gr., porphyritic biotite-hornblende granodiorite; local clinopyroxene; mafic enclaves common; locally forms net-veined complexes with gabbro and dolerite.||||||07-FEB-11
21229|Bend Granodiorite|22847|3|Fully described|p 43|Ordovician|Early Ordovician|||||||
21229|Bend Granodiorite|23422|6|Mentioned|p209 Table 6.6|||||||||
21229|Bend Granodiorite|23504|5|Briefly described|Map Legend||Ordovician|||||||
21229|Bend Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 491. I-Type.||||||
21229|Bend Granodiorite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Probable Early to Middle Ordivician||||||
21229|Bend Granodiorite|43259|4|Described|Appendix 1,p51.||Ordovician|Ordovician?||||||27-AUG-08
21229|Bend Granodiorite|43936|5|Briefly described|Map Legend||Ordovician|||||||
21252|Billycan Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Age: 300 +/- 1Ma, Rb-Sr. Ootann Supersuite.||||||
21252|Billycan Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21252|Billycan Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 318. I-Type.||||||
21252|Billycan Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
21252|Billycan Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
21252|Billycan Granite|43087|2|Defined|p27|Late Carboniferous||Of Ootann Suite of Richards (1981) and Ootann Supersuite of Champion (1991).||||||
21252|Billycan Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21252|Billycan Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|Late? Carboniferous in age.||||||
21252|Billycan Granite|43626|6|Mentioned|p10|||||||||
21252|Billycan Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pink medium-gr., even-gr. biotite granite; leucocratic; accessory apatite, zircon, magnetite with ilmenite exsolution lamellae; rare inclusions (most <2cm across).||||||07-FEB-11
21252|Billycan Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.|301-302 Ma (Rb-Sr, biotite).|Unit in Ootann Supersuite.|||Pink, medium-grained, leucocratic biotite monzogranite to syenogranite.|
21269|Blanders Granodiorite|23032|5|Briefly described|p39|||||||||
21269|Blanders Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
21269|Blanders Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
21269|Blanders Granodiorite|43480|2|Defined|16-26|Devonian|Silurian|||||||
21269|Blanders Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Grey, foliated, medium-grained hornblende-biotite granodiorite.|
21269|Blanders Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Grey, foliated, medium-grained hornblende-biotite granodiorite.|
21269|Blanders Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
21273|Bluewater Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
21273|Bluewater Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 306+/-3 Ma, Rb-Sr. of Boonmoo Volcanic Subgroup.||||||
21273|Bluewater Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group. Age: 306+/-3Ma.||||||
21273|Bluewater Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V133. I-Type.||||||
21273|Bluewater Rhyolite|23616|5|Briefly described|Table 3 p49||Carboniferous|Age: 306+/-3 Ma (Rb-Sr). Of Boonmoo Volcanic Subgroup.||||||
21273|Bluewater Rhyolite|43060|5|Briefly described|Table 5|||Of Featherbed Volcanic Group.||||||03-JUN-09
21273|Bluewater Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).  Rhyodacitic to rhyolitic ignimbrite with orthopyroxenes in places.  Age: 306+/-3Ma.||||||15-JUN-06
21273|Bluewater Rhyolite|43259|4|Described|Appendix 1,p14.||Late Carboniferous|Of Boonmoo Volcanic Subgroup. Age is 306+/-3 Ma.||||||03-JUN-09
21273|Bluewater Rhyolite|43567|5|Briefly described|Table 2,p401|||||||||
21273|Bluewater Rhyolite|43626|2|Defined|p21||Late Carboniferous|Rb-Sr dating (306+/-3 Ma).||||||03-JUN-09
21273|Bluewater Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21273|Bluewater Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21273|Bluewater Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Boonmoo Volcanic Subgroup.|||Dark grey to bluish or greenish grey, welded, augite-hornblende-biotite rhyodacitic to rhyolitic ignimbrite, with orthopyroxene in places and rare clasts of rhyolite.|
21273|Bluewater Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|305 Ma.|Featherbed Volcanic Group.||||
21273|Bluewater Rhyolite|71592|5|Briefly described|Appendix A.|||Kennedy igneous Province.|308+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
21277|Bock Granodiorite|23423|6|Mentioned|p306 Table 7.3|||||||||
21277|Bock Granodiorite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of Almaden Supersuite.||||||02-JUN-09
21277|Bock Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 278. I-Type.||||||
21277|Bock Granodiorite|23616|6|Mentioned|Table 3 p48|||||||||
21277|Bock Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).||||||15-JUN-06
21277|Bock Granodiorite|43259|4|Described|Appendix 1,p35.||Late Carboniferous|||||||
21277|Bock Granodiorite|60425|4|Described|p49 Tb.3, p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Intruded Boonmoo Volcanic Subgroup. I-type. Dark grey, fine to medium-grained, slightly porphyritic augite-biotite-hornblende granodiorite.||||||07-FEB-11
21357|Bulgin Creek Granite|22630|5|Briefly described|p21|||Lolworth Batholith||||||
21357|Bulgin Creek Granite|22844|6|Mentioned|p21|Devonian|Silurian|Part of the Lolworth Batholith.||||||
21357|Bulgin Creek Granite|23049|3|Fully described|p41|Early Devonian|Late Silurian|of Hodgon Suite.||||||
21357|Bulgin Creek Granite|23283|2|Defined|p21|Devonian|Silurian|||||||
21357|Bulgin Creek Granite|23422|4|Described|p216 Table 6.10|Early Devonian|Late Silurian|Of Amarra Supersuite.||||||
21357|Bulgin Creek Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Hodgon Suite||||||
21368|Bulluburrah Granodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite?||||||
21368|Bulluburrah Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 433. I-Type.||||||
21368|Bulluburrah Granodiorite|23616|6|Mentioned|Table 3 p51|||||||||
21368|Bulluburrah Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21368|Bulluburrah Granodiorite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
21368|Bulluburrah Granodiorite|60425|4|Described|p49 Tb.3, p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Comprises 2 subunits: (1) a highly porphyritic hornblende-biotite microgranodiorite to microgranite, and (2) pyroxene?-biotite-hornblende gabbro. Additional lithologcal details included. Cut into Beapeo Rhyolite.||||||30-MAR-15
21369|Bulonga Volcanics|67323|5|Briefly described|p16-17, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Forms the core of the Mitakoodi Domain, Mount Isa Inlier, Leichhardt Superbasin. Originally mapped as Argylla Formation (Derrick, 1980). High magnetic susceptibility; moderate U-K-Th radiometric response; low gravity response. Both age determinations from the Geoscience Australia OZCHRON database.|1762 +/- 5 Ma and 1758 +/- 4 Ma.|||Is overlain by Marraba Volcanics. May be thrust over the Corella Formation. Is intruded by Levian Granite.|Porphyritic or crystal-rich rhyolitic to dacitic metavolcanics, feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss.|
21369|Bulonga Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
21369|Bulonga Volcanics|69056|4|Described|p2-4, p6, p13, p18, p23, p28, p52-53|Statherian|Statherian|See also Time-Space plot sheet, Reference images sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area. Basement in the Soldiers Cap Domain; cover sequence elsewhere. In the Mitakoodi Domain, previously mapped as Argylla Formation (Derrick, 1980). Modelling values listed.|1762 +/- 5 Ma.|||Overlies Argylla Formation. Is overlain by Corella and Staveley Formations and Marraba Volcanics.|Felsic volcanics and metavolcanics.|
21369|Bulonga Volcanics|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic or crystal-rich rhyolite to dacite, feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss (subsurface)|
21369|Bulonga Volcanics|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic or crystal-rich rhyolite to dacite, feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss|
21369|Bulonga Volcanics|69591|5|Briefly described|p29, p33, p50 Fig.2.42|Paleoproterozoic|Paleoproterozoic|Mitakoodi Domain, Leichhardt Superbasin, Mount Isa Province.|1761 Ma.||||Felsic.|
21369|Bulonga Volcanics|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic or crystal-rich rhyolite to dacite (including ignimbrite), commonly magnetite-bearing.|
21369|Bulonga Volcanics|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||||Porphyritic or crystal-rich rhyolite to dacite (including ignimbrite), commonly magnetite-bearing.|
21369|Bulonga Volcanics|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Porphyritic to crystal-rich rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss.|
21369|Bulonga Volcanics|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Three facies are mapped separately.|||||Porphyritic to crystal-rich rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss.|
21369|Bulonga Volcanics|71799|5|Briefly described|p150 fig 2, p151 fig 3, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block. Petrographically and compositionally indistinguishable with the Argylla Formation.|ca. 1760 Ma|||Overlain by the Marraba Volcanics.|Silicic volcanics, porphyry.|
21369|Bulonga Volcanics|72596|6|Mentioned|p24|Statherian|Statherian|Geochronologic constraint from a rhyolite, rhyodacite and recrystallised felsic volcanics; see Geoscience Australia, 2011: Sample ID 95208079, [unknown], and 2006169006, respectively. Neumann et al. (2009) included the 2006 sample in the Argylla Formation.|1762 +/- 3 Ma, 1761 +/- 4 Ma, 1754 +/- 8 Ma|||||
21369|Bulonga Volcanics|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Comprised of 3 informal lithological divisions within unit.|||||Porphyritic or crystal-rich rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss. Includes medium to coarse-grained quartzite and feldspathic sandstone; rhyolite.|
21369|Bulonga Volcanics|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Comprised of 3 informal lithological divisions within unit.|||||Porphyritic or crystal-rich rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss. Includes Medium to coarse-grained quartzite and feldspathic sandstone; rhyolite.|
21369|Bulonga Volcanics|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Two informal sub-units described.||||Shown as older than the Malbon Group and younger than the Argylla Formation.|Porphyritic  or crystal-rich rhyolite rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss.|
21369|Bulonga Volcanics|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Two informal sub-units described including a porphyritic or crystal-rich rhyolite to dacite and feldspathic to quartzose, locally micaceous metasandstone and siltstone.||||Shown as older than the Malbon Group and younger than the Argylla Formation.|Porphyritic or crystal-rich rhyolite to dacite (including ignimbrite), feldspathic to quartzose metasandstone, grading locally into muscovite-biotite schist and gneiss.|23-JUL-20
21369|Bulonga Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
21369|Bulonga Volcanics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
21369|Bulonga Volcanics|73525|5|Briefly described|p2 Fig.1, p4|Statherian|Statherian|Mitakoodi-Tommy Creek Domains.|1762+/-5 Ma, 1761+/-4 Ma crystallisation age||||Felsic extrusives.|
21369|Bulonga Volcanics|73553|6|Mentioned|p263|||||||Intruded by Wimberu Granite||
21373|Bungabilly Granite|23423|6|Mentioned|p307 Table 7.3|||||||||
21373|Bungabilly Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21373|Bungabilly Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21373|Bungabilly Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 434. I-Type.||||||
21373|Bungabilly Granite|23616|5|Briefly described|Table 3 p52, p99 Appen. 2||Carboniferous|Of Ootann Supersuite.||||||
21373|Bungabilly Granite|23713|5|Briefly described|p72 Appendix 2|||||||||
21373|Bungabilly Granite|24485|5|Briefly described|p43 Tb.7|Late Carboniferous|Late Carboniferous|Parent: Ootann Supersuite. Extensively intrudes the Doolan Creek Rhyolite||||||
21373|Bungabilly Granite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
21373|Bungabilly Granite|43060|5|Briefly described|Table 6|||of Ootann Supersuite||||||
21373|Bungabilly Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
21373|Bungabilly Granite|43087|6|Mentioned|Fig.5|||See also Bungabilly Adamellite, p75.||||||
21373|Bungabilly Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). .||||||15-JUN-06
21373|Bungabilly Granite|43254|5|Briefly described|map legend||Late Carboniferous|of Ootann Supersuite.||||||
21373|Bungabilly Granite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
21373|Bungabilly Granite|43285|5|Briefly described|Map Legend||Late Carboniferous|||||||
21373|Bungabilly Granite|43625|6|Mentioned|p21|||||||||
21373|Bungabilly Granite|60425|4|Described|p49 Tb.3, p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Med.-to coarse-gr., even-gr., to slightly porphyritic, leucocratic (hornblende-) biotite granite, with sparse mafic enclaves to 5cm; minor aplitic biotite microgranite, aplite. Intruded Doolan Creek Rhyolite.||||||07-FEB-11
21373|Bungabilly Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pale pink, medium- to coarse-grained, even-grained to slightly porphyritic, leucocratic (hornblende-)biotite monzogranite, with sparse mafic enclaves to 5 cm; minor aplitic biotite microgranite, aplite.|
21399|Burunga Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
21399|Burunga Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
21399|Burunga Formation|43483|6|Mentioned|13-14||Permian|||||||
21399|Burunga Formation|61076|5|Briefly described|p188 Fig. 2|Late Permian|Late Permian|Includes the Scotia Member. Age: >250Ma. Geological Province: Bowen Basin, Taroom Trough.||||||05-JUN-06
21399|Burunga Formation|62357|5|Briefly described|p524 Fig. 7|Late Permian|Late Permian|Includes the Scotia Member. Geological Province: Bowen Basin.||||||
21399|Burunga Formation|64665|6|Mentioned|p52.|Permian|Permian|Bowen Basin.||||||
21399|Burunga Formation|64856|4|Described|p42, p57 Fig.8, p58-62, p65-67, p102|Late Permian|Late Permian|Beeston and Green (1995). Bowen Basin. In the S of the study area, this name is applied to the combined Tinowon-Bandanna Formations interval. Equivalent to upper part of Gyranda Formation, laterally equivalent to Wiseman Formation. Includes basal Scotia Coal Member. Conformably overlies the Banana Formation and Muggleton Formation. Age from palynoflora (unit APP5). 677m thick.|| |||Sandstone, siltstone, tuff, coal, shale. Includes marine shells and poorly preserved plant material throughout.|28-NOV-17
21399|Burunga Formation|64857|5|Briefly described|p119, 121-124, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Overlies Muggleton Formation.||||||
21399|Burunga Formation|64858|5|Briefly described|p182, p180 Fig.2, p186 Fig.10|Late Permian|Late Permian|Bowen Basin. Contains Scotia (Coal) Member. Includes coal. Overlies Banana Formation. Southern Taroom Trough.||||||16-MAR-12
21399|Burunga Formation|64859|5|Briefly described|p196, 225|Permian|Permian|Contains Scotia Coal Member. Oil and gas source rocks.||||||
21399|Burunga Formation|65112|5|Briefly described|p315, Fig 4 p314|Late Permian|Late Permian|Part of Supersequence F. In Bowen-Gunnedah-Sydney Basin system in the Taroom Trough, a 4 Ma sequence up to 500 m thick in east. Called the Black Alley Shale in Denison Trough.|||Includes basal Scotia Coal Member.|Underlies the Baralaba Coal Measures.||22-MAR-12
21399|Burunga Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Taroom Trough. Overlies Scotia Coal Member, underlies Baralaba Coal Measures.||||||
21399|Burunga Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
21399|Burunga Formation|65115|5|Briefly described|p415, 418, 420, Fig 2 p403|Permian|Permian|Includes basal Scotia Coal Member, underlies the Baralaba Coal Measures in the Taroom Trough, Bowen Basin. Part of Supersequence E (Scotia Coal Member), and F.||||||
21399|Burunga Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Baralaba CM and overlies the Scotia Coal Member in the Taroom Trough, Bowen Basin.||||||23-MAR-12
21399|Burunga Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Baralaba Coal Measures in the Taroom Trough, Bowen Basin. Includes the Scotia Member||||||
21399|Burunga Formation|65119|6|Mentioned|Fig 6 p512, Fig 14 p521|||Present in the Burunga 1 and MacIntyre 1 wells.||||||07-MAR-12
21399|Burunga Formation|66615|6|Mentioned|p2 Fig.1, p4 Fig.2, p5 Fig.3, p6-8|||Southern Taroom Trough, Bowen Basin. Has marine and coal facies.|||Includes Scotia Coal Member.|||
21399|Burunga Formation|67402|5|Briefly described|p21, p45, p52|Wuchiapingian|Wuchiapingian|Bowen Basin. Generally greater than 100m thick. See also p57 tbl BWS3, p165 tbl LPB1.||||Overlain by the Baralaba Coal Measures. Overlies the Banana Formation, Flat Top Formation and the Barfield Formation.|Intraformational siltstones, mudstones and tuffs.|
21399|Burunga Formation|68679|5|Briefly described|p377, p381-384|Permian|Permian|Beeston and Green (1995). Eastern Taroom Trough, Bowen Basin. 677m thick. Delta, offshore marine (transgressive), prodelta sediments. Properties of the coal are described in some detail.|||Scotia Coal Member.|Overlies Banana Formation. Is overlain by Baralaba Coal Measures.|Fine- to medium-grained, poorly sorted sandstone, volcaniclastic conglomerate, shale, siltstone, coal and tuff; marine shells present.|
21399|Burunga Formation|72297|5|Briefly described|p744|||Bowen Basin. Oil and gas producer.|||Scotia Coal Member.||Includes coal, mudstone.|
21404|Buthen Buthen Granite|43741|3|Fully described|p10|Devonian|Silurian|Age: approx 407 Ma. 'informal unit'||||||
21404|Buthen Buthen Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
21404|Buthen Buthen Granite|71792|3|Fully described|p5, p26-p27, p59|Lower Devonian|Late Silurian|Named for the Buthen Buthen Mine in the Hayes Creek gold field. No type area has been defined. Defined by Knutson et al, 1994 after formerly being mapped as part of the Kintore Granite. This unit is inacessible as a result of lack of roads, dense jungle and its location east of a major river valley and is described almost exclusively from the area surrounding the Buthen Buthen Mine. Forms a series of prominent ranges, east of the Lockhart River Valley. Exhibits a moderate to low mottled response in magnetic imagery with some lineations interpreted as faults. The radiometric response is variable; most of the unit is high in potassium with a mottled texture.||Kintore Supersuite||Intrudes the Newberry Metamorphic Group and the Coen Metamorphic Group. Intruded by the Cape Weymouth Granite. Faulted against the McIlwraith Granite.|Subdivided into two lithologically separate granites a light grey, medium-grained leucogranite and a biotite-muscovite leucogranite that is largely coarse grained.|09-AUG-18
21404|Buthen Buthen Granite|71849|3|Fully described|p3,p8,p13,p50-57,p152-153,p161-162,p195|Devonian|Devonian|See also p150. Previously part of the Kintore Adamellite (Trail et al., 1994 and others); later the (informal) Buthen Buthen granite of Knutson et al. (1994). NNE of Coen. Forms a prominent belt of relatively high mountainous country. Proposed type area is around MGA 769222 8520471. Named after Buthen Buthen Creek and the abandoned mine of the same name. Not mapped in detail. Geophysics, geochemistry described. Lithologies, photomicrographs detailed. Local inclusions of country rock up to several metres long. Not isotopically dated; age inferred from overall similarity to Kintore Supersuite granitoids.||Buthen Buthen Suite.||Intrudes Coen Metamorphic Group. Is intruded by Weymouth Supersuite. Is overlain nonconformably by Lilyvale beds.|White-pale grey, mainly medium-grained, even-grained to moderately porphyritic muscovite-biotite and biotite-muscovite granite to granodiorite; generally deformed with well-developed foliation. Minor pegmatite, aplite, leucogranite.|10-APR-19
21404|Buthen Buthen Granite|71853|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Buthen Buthen Suite.|||Muscovite-biotite and biotite-muscovite leucogranite.|
21404|Buthen Buthen Granite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Buthen Buthen Suite.|||Muscovite-biotite and biotite-muscovite leucogranite.|
21438|Capel Granodiorite|23032|5|Briefly described|p40|Early Devonian||K/Ar Age: 403+/-10 Ma (must be a minimum age).||||||
21438|Capel Granodiorite|23422|6|Mentioned|p215 Table 6.9|||||||||
21438|Capel Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
21438|Capel Granodiorite|43480|2|Defined|7-64|Devonian|Silurian|K-Ar Age: 403+/-10Ma||||||
21438|Capel Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Foliated buff, grey or pinkish-grey,  medium-grained, sparsely porphyritic muscovite-biotite granodiorite, with alkali feldspar phenocrysts up to 3cm.||||||
21438|Capel Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Foliated buff, grey or pinkish-grey, medium-grained sparsely porphyritic muscovite-biotite granodiorite, with alkali feldspar phenocrysts up to 3 cm.|
21438|Capel Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Foliated buff, grey or pinkish-grey, medium-grained sparsely porphyritic muscovite-biotite granodiorite, with alkali feldspar phenocrysts up to 3 cm.|
21438|Capel Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Foliated buff, grey or pinkish-grey, medium-grained sparsely porphyritic muscovite-biotite granodiorite, with alkali feldspar phenocrysts up to 3 cm.|
21438|Capel Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.|403 +/- 10 Ma (K-Ar, biotite).|Upland Supersuite.|||I-type.|
21463|Carysfort Quartzite|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Holroyd Group||||||12-JAN-05
21463|Carysfort Quartzite|22781|4|Described|p20|Proterozoic|Proterozoic|Holroyd Group||||||
21463|Carysfort Quartzite|23420|5|Briefly described|p 143 table 4.4|||In the Holroyd Group, Coen Inlier. Thickness 1000m||||||
21463|Carysfort Quartzite|43596|4|Described|p19 Tb. 1, p22|Mesoproterozoic|Mesoproterozoic|Of Holroyd Group. Max. thickness: ~1000m. Conformable on Astrea Fm; overlain by Newirie Fm. Intruded by Culpin Granite. Dominantly quartzite, fine- to v. fine-gr. quartzite - lithological details included.||||||15-JAN-09
21463|Carysfort Quartzite|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Holroyd Group.||||||24-JAN-05
21463|Carysfort Quartzite|69591|5|Briefly described|p79 Tb.2.6|||Savannah Province, Coen Inlier. 1000m thick. Occurs in a small area N of Astrea homestead and Potallah Creek.||Holroyd Group.||Interfingers with Newirie Formation.|Quartzite, phyllite, graphite schist, slate. More pelitic to the south.|
21488|Chelmsford Gneiss|23420|5|Briefly described|p 144 table 4.4||Mesoproterozoic|In the Yambo Metamorphic Group, Yambo Subprovince. Age: ~1580Ma. Outcrops in the eastern part of the Yambo Inlier.||||||
21488|Chelmsford Gneiss|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group. Age: ~1585Ma (SHRIMP).||||||
21488|Chelmsford Gneiss|23511|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
21488|Chelmsford Gneiss|23713|4|Described|p9 Table 1 + p10||Mesoproterozoic|Of Yambo Metamorphic Group. Overlying unit Mitchell River Volcanics and Gilbert River Formation - unconformable. Yambo Province.||||||
21488|Chelmsford Gneiss|43254|5|Briefly described|map legend||Mesoproterozoic|of Yambo Metamorphic Group.||||||
21488|Chelmsford Gneiss|43285|5|Briefly described|Map Legend|||age Middle Proterozoic.||||||
21488|Chelmsford Gneiss|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
21488|Chelmsford Gneiss|43596|4|Described|p8, p13-14, p20 Tb. 1||Proterozoic|Of Yambo Metamorphic Group.  Predominantly medium-grained sillimanite-biotite-quartzofeldspathic gneiss and intercalated biotite-quartzofeldspathic gneiss. Andalusite, cordierite and K-feldspar are rare, garent porphyroblasts common. Detailed lith. given.||||||07-APR-15
21488|Chelmsford Gneiss|43625|3|Fully described|p15,Table 1||Mesoproterozoic|Age: approx 1580-1590 Ma||||||
21488|Chelmsford Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Yambo Metamorphic Group||||||24-JAN-05
21488|Chelmsford Gneiss|60357|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Geological Province: Yambo Subprovince. Of the Yambo Metamorphic Group.||||||07-NOV-08
21488|Chelmsford Gneiss|60358|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Sillimanite-biotite gneiss, augen gneiss, migmatitic gneiss; minor quartzite, amphibolite, mafic granulite, granite. Geological Province: Yambo Subprovince.||||||07-NOV-08
21488|Chelmsford Gneiss|69591|5|Briefly described|p71 Fig.2.69, p72|Paleoproterozoic|Paleoproterozoic|Yambo Inlier. Similar lithologies to Pombete Gneiss. Underwent upper amphibolite to granulite grade regional metamorphism.|1584 +/- 2 Ma (mafic granulite protolith).|Yambo Metamorphic Group.|||Sillimanite-biotite(+/- garnet) quartzofeldspathic gneiss; quartzite, garnet quartzite, two-mica granite, hornblende amphibolite and two-pyroxene mafic granulite.|
21488|Chelmsford Gneiss|69592|6|Mentioned|p233|Proterozoic|Proterozoic|||||||
21488|Chelmsford Gneiss|71031|6|Mentioned|p71|Mesoproterozoic|Palaeoproterozoic|||||||
21488|Chelmsford Gneiss|73083|6|Mentioned|p67, p76|||||||||
21498|Chippendale Granodiorite|22847|3|Fully described|p 52|Late Silurian||||||||
21498|Chippendale Granodiorite|23422|5|Briefly described|p176, p213 Table 6.8|Silurian|Silurian|Of Millchester Supersuite.||||||
21498|Chippendale Granodiorite|23430|5|Briefly described|Table 14.2 p460.||Silurian|K-Ar; Rb-Sr 411 +/- 2 Ma. Ravenswood Batholith Province||||||
21498|Chippendale Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
21498|Chippendale Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 199. I-Type.||||||
21498|Chippendale Granodiorite|43093|4|Described|Appendix 1|||Rb/Sr biotite age of 411+/-2Ma.||||||
21498|Chippendale Granodiorite|43259|4|Described|Appendix 1,p29.||Late Silurian|Mb-Sr age is 411+/-2 Ma.||||||
21498|Chippendale Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
21498|Chippendale Granodiorite|62075|6|Mentioned|p15 Fig.7|Late Silurian|Late Silurian|Ravenswood batholith. Appears as Chippendale granodiorite.||||||
21499|Chuko Quartzite|23420|5|Briefly described|p 145 table 4.4|||In the Yambo Metamorphic Group, Yambo Subprovince.||||||
21499|Chuko Quartzite|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
21499|Chuko Quartzite|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
21499|Chuko Quartzite|69591|6|Mentioned|p71 Fig.2.69|||Yambo Inlier.||||||
21523|Combella Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Yongala Volcanic Subgroup of Featherbed Volcanic Group.||||||
21523|Combella Rhyolite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup. Age: 284+/-4Ma Rb-Sr.||||||
21523|Combella Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Age: 284+/-4 Ma, Rb-Sr. Of Yongala Volcanic Subgroup and Lags Supersuite.||||||
21523|Combella Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V110. A-Type.||||||
21523|Combella Rhyolite|23616|5|Briefly described|Table 3 p47||Permian|Age: 284+/-4 Ma (Rb-Sr). Of Yongala Volcanic Subgroup/Featherbed Volcanic Group.||||||
21523|Combella Rhyolite|23713|5|Briefly described|p22|||Age: 284+/-4 Ma (Rb-Sr isotope). Overlying unit Arringunna Rhyolite.||||||
21523|Combella Rhyolite|43060|5|Briefly described|Table 5|||of Featherbed Volcanic Group||||||
21523|Combella Rhyolite|43083|5|Briefly described|p92|||Age: 284+/-4 Ma (Rb-Sr). Of Featherbed Volcanic Group||||||17-JUN-09
21523|Combella Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup (Featherbed Volcanic Group).  Age: 284+/-4Ma.||||||15-JUN-06
21523|Combella Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Yongala Volcanic Subgroup. Age 284+/-4 Ma.||||||
21523|Combella Rhyolite|43259|4|Described|Appendix 1,p11.||Early Permian|of Yongala Volcanic Subgroup. Age is 284+/-4 Ma.||||||
21523|Combella Rhyolite|43285|5|Briefly described|Map Legend||Permian|of Featherbed Volcanic Subgroup.||||||
21523|Combella Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
21523|Combella Rhyolite|43626|2|Defined|p50||Early Permian|Rb-Sr age: 284+/-4 Ma (average from 2 samples).||||||02-APR-15
21523|Combella Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
21523|Combella Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Age: 284 +/- 4 Ma (Rb-Sr). Of Yongala Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
21523|Combella Rhyolite|60425|5|Briefly described|p46 Tb. 3|Early Permian|Early Permian|Of the Yongala Volcanic Subgroup (Featherbed Volcanic Group). Age: 284+/-4Ma (Rb-Sr).||||||07-FEB-11
21523|Combella Rhyolite|62523|6|Mentioned|p19 Tb.2|||In central Featherbed Cauldron.||||||07-FEB-11
21523|Combella Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province. Another sub-unit, also separately mapped, is locally lithics-rich with 1 m thick vitrophyre zone at base, minor flow-banded, slightly porphyritic rhyolite.|283 +/- 5 Ma (Rb-Sr, total rock).|Unit in Yongala Volcanic Subgroup.|||Variably welded and altered, crystal-poor to moderately crystal-rich, rhyolitic ignimbrite, commonly spherulitic, extensive vitrophyre zones, rare rhyolitic lava; locally spheruloid ('thunder egg')-rich ignimbrite.|
21523|Combella Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Included in Lags Supersuite.|284 Ma.|Featherbed Volcanic Group.|||A-type.|
21534|Controversy Hill Rhyolite|23423|5|Briefly described|p306 Table 7.3|Early Permian|Late Carboniferous|Timber Top Volcanic Subgroup of Featherbed Volcanic Group.||||||
21534|Controversy Hill Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21534|Controversy Hill Rhyolite|43259|6|Mentioned|Appendix 1,p11.|Early Permian|Late Carboniferous|||||||
21534|Controversy Hill Rhyolite|43567|5|Briefly described|Table 1,p400|||||||||
21534|Controversy Hill Rhyolite|43625|6|Mentioned|p36|||||||||
21534|Controversy Hill Rhyolite|43626|6|Mentioned|Table 1, p15|||||||||
21534|Controversy Hill Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgroup. Geological Province: Kennedy Province.||||||
21534|Controversy Hill Rhyolite|60425|5|Briefly described|p46 Tb. 3||Early Permian|Of Timber Top Volcanic Subgroup (Featherbed Volcanic Group). A-type rocks.||||||07-FEB-11
21534|Controversy Hill Rhyolite|62523|4|Described|p3-4, p4-5|Early Permian|Late Carboniferous|Of Timber Top Volcanic Subgrp. Mainly rhyolite and dacite (detailed lithology given). Assoc.with Maneater Granodiorite, in places intruded by it. Intrudes Breccia Creek Rhyolite; together with this unit these form irreg. ring-dyke around Mulligan Cauldron||||||07-FEB-11
21535|Convict Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite||||||
21535|Convict Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 439. I-Type.||||||
21535|Convict Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
21535|Convict Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21535|Convict Granite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
21535|Convict Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Very pale grey, cream or white, medium to coarse-grained, biotite leucogranite; with sparse W-Mo mineralisation; cut by aplite dykes, and quartz veins and pipes.||||||07-FEB-11
21535|Convict Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Very pale grey, cream or white, medium- to coarse-grained biotite leucogranite; cut by aplite dykes and quartz veins and pipes.|
21565|Cottell Rhyolite|23423|6|Mentioned|p306 Table 7.3|||||||||
21565|Cottell Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: 300+/-1 Ma, Rb-Sr. Of Ootann Supersuite.||||||30-MAR-15
21565|Cottell Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 436. I-Type.||||||
21565|Cottell Rhyolite|23616|6|Mentioned|Table 3 p48|||||||||
21565|Cottell Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21565|Cottell Rhyolite|43259|4|Described|Appendix 1,p47.||Carboniferous|Age is 301 Ma.||||||
21565|Cottell Rhyolite|43567|5|Briefly described|Table 2,p401|||||||||
21565|Cottell Rhyolite|43626|6|Mentioned|p11|||||||||
21565|Cottell Rhyolite|60425|4|Described|p49 Tb.3, p278-9 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Ste (Ootann Sup'ste). Intruded Boonmoo Volc. Subgp. I-type. Divided into (1) fine- to med.gr., variably porph'ic rhyolite (spherulitic in places); (2) mod'ly crystal-poor, intrusive rhyolitic ignimbrite; minor rhyolite breccia, polymictic breccia.||||||30-MAR-15
21565|Cottell Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. A sub-unit of pink to pinkish grey, moderately crystal-poor, rhyolitic ignimbrite (intrusive), is mapped separately.||Unit in Ootann Supersuite.|||Pale brown, buff, white or grey, fine- to medium-grained, variably porphyritic biotite rhyolite (intrusive: spherulitic in places); minor rhyolitic ignimbrite, rhyolite breccia, polymictic breccia.|
21571|Cracknell Granodiorite|23032|5|Briefly described|p40|||||||||
21571|Cracknell Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
21571|Cracknell Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
21571|Cracknell Granodiorite|43480|2|Defined|7-36|Devonian|Silurian|||||||
21571|Cracknell Granodiorite|68478|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Pinkish grey, foliated, medium-grained, porphyritic muscovite-biotite granodiorite.|
21571|Cracknell Granodiorite|68479|5|Briefly described|Map Legend|Early Devonian|Silurian|Reedy Springs Batholith, Pama Province.|||||Pinkish grey, foliated, medium-grained, porphyritic muscovite-biotite granodiorite.|
21571|Cracknell Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
21577|Crescent Granodiorite|22847|3|Fully described|p 54|Early Devonian|Late Silurian|||||||
21577|Crescent Granodiorite|23504|5|Briefly described|Map Legend|Devonian|Silurian|||||||
21577|Crescent Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 185. I-Type||||||
21577|Crescent Granodiorite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
21577|Crescent Granodiorite|43259|4|Described|Appendix 1,p28.|Early Devonian|Late Silurian|||||||
21577|Crescent Granodiorite|43935|5|Briefly described|Map Legend|Devonian|Silurian|||||||
21577|Crescent Granodiorite|43936|5|Briefly described|Map Legend|Devonian|Silurian|||||||
21577|Crescent Granodiorite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Crescent gdrt.||Unit in Millchester Supersuite.||||
21588|Cummings Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|Of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||03-JUN-09
21588|Cummings Rhyolite|23513|5|Briefly described|Map legend||Late Carboniferous|Palaeozoic Volcanic No. V92. I-Type.||||||
21588|Cummings Rhyolite|23616|5|Briefly described|Table 3 p49||Carboniferous|Of Boonmoo Volcanic Subgroup.||||||03-JUN-09
21588|Cummings Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21588|Cummings Rhyolite|43259|4|Described|Appendix 1,p9.||Late Carboniferous|Of Boonmoo Volcanic Subgroup.||||||
21588|Cummings Rhyolite|43626|3|Fully described|p21||Late Carboniferous|Age: 313 Ma||||||
21588|Cummings Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21588|Cummings Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21604|Daintree Gneiss|23420|5|Briefly described|p 144 table 4.4|||In the Yambo Metamorphic Group. Partly correlates with Arkara Gneiss.||||||
21604|Daintree Gneiss|23496|5|Briefly described|Table 1||Proterozoic|of Yambo Metamorphic Group.||||||
21604|Daintree Gneiss|43287|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
21604|Daintree Gneiss|43596|4|Described|p8, p13-14, p20 Tb. 1||Proterozoic|Of Yambo Metamorphic Group. Intruded by Fernhill Granite and Lukinville Granodiorite. Predominantly biotite-rich quartzofeldspathic gneiss with scarce sillimanite; generally medium- to coarse-grained. Detailed lithology provided.||||||15-JAN-09
21604|Daintree Gneiss|43820|5|Briefly described|Map Legend||Mesoproterozoic|of Yambo Metamorphic Group||||||24-JAN-05
21604|Daintree Gneiss|69591|5|Briefly described|p71 Fig.2.69, p72 Tb.2.3|Paleoproterozoic|Paleoproterozoic|Yambo Inlier.||Yambo Metamorphic Group.||May partly correlate with Arkara Gneiss.|Garnet-biotite quartzofeldspathic gneiss; lesser hornblende amphibolite.|
21609|Dalnotter Dacite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Tennyson Volcanic Subgroup of Featherbed Volcanic Group.||||||
21609|Dalnotter Dacite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Tennyson Volcanic Subgroup.||||||
21609|Dalnotter Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. 125. I-Type.||||||
21609|Dalnotter Dacite|23616|5|Briefly described|Table 3 p48||Late Carboniferous|Of Tennyson Volcanic Subgroup.||||||
21609|Dalnotter Dacite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|O the Tennyson Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21609|Dalnotter Dacite|43259|4|Described|Appendix 1,p13.||Late Carboniferous|Of Koorboora Volcanic Subgroup.||||||03-JUN-09
21609|Dalnotter Dacite|43567|5|Briefly described|Table 2,p400|||||||||
21609|Dalnotter Dacite|43626|2|Defined|p30|Early Permian|Late Carboniferous|Between 289+/-7 Ma and 306+/-3 Ma.||||||03-JUN-09
21609|Dalnotter Dacite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21609|Dalnotter Dacite|60425|5|Briefly described|p46 Tb. 3|Late Carboniferous|Late Carboniferous|Of Tennyson Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21609|Dalnotter Dacite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Tennyson Volcanic Subgroup.|||Dark grey to greenish grey, welded, crystal-rich to very crystal-rich, hornblende-biotite dacitic ignimbrite; with fiamme to 10 cm; locally lithics-poor to lithics-rich (especially at base).|
21622|Davey Creek Granite|23049|3|Fully described|p23|Early Devonian|Late Silurian|400+/-12Ma||||||
21622|Davey Creek Granite|23283|2|Defined|p20|Devonian|Silurian|||||||
21622|Davey Creek Granite|23422|5|Briefly described|p177, p216 Table 6.10|Middle Devonian|Early Devonian|Of Amarra Supersuite.||||||
21622|Davey Creek Granite|23430|5|Briefly described|Table 14.2 p460.||Devonian|K-Ar; Rb-Sr 400 +/- 12 Ma and 408 +/- 7 Ma. Lolworth Batholith Province||||||
21622|Davey Creek Granite|23499|5|Briefly described|map legend|Devonian|Silurian|Lolworth Batholith.||||||
21622|Davey Creek Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
21622|Davey Creek Granite|69592|5|Briefly described|p292-293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~45 km2. Similar to Amarra Granite. K-Ar (biotite) and K-Ar (muscovite) ages by Webb (1971) and Hutton, Garrad and Withnall (1995).|404 +/- 12 Ma; 400 +/- 12 Ma.|Amarra Suite.|||Mainly pink to grey even-grained biotite and muscovite-biotite granite.|
21632|Deadman Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
21632|Deadman Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 277. I-Type.||||||
21632|Deadman Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
21632|Deadman Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21632|Deadman Granite|43259|4|Described|Appendix 1,p35.||Late Carboniferous|||||||
21632|Deadman Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Pale to medium grey or pinkish grey, highly porphyritic biotite microgranite. Also referred to informally as Deadman granite (p287) as name once assigned to Whelan Creek Granite.||||||07-FEB-11
21634|Deep Water Creek Granophyre|22630|5|Briefly described|p37|||||||||
21634|Deep Water Creek Granophyre|22844|6|Mentioned|p37|Permian|Carboniferous|||||||
21634|Deep Water Creek Granophyre|23049|3|Fully described|p67|||Probably Carboniferous or Permian in age||||||
21634|Deep Water Creek Granophyre|23283|2|Defined|p30|Permian|Carboniferous|||||||
21634|Deep Water Creek Granophyre|23499|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
21660|Dillons Knob Granite|23049|3|Fully described|p21-22|Early Devonian|Late Silurian|Age: ~400-409Ma.||||||
21660|Dillons Knob Granite|23283|2|Defined|p20|Devonian|Silurian|||||||
21660|Dillons Knob Granite|23422|4|Described|p216 Table 6.10|Early Devonian|Late Silurian|Of Amarra Supersuite.||||||
21660|Dillons Knob Granite|23508|5|Briefly described|Map Legend|Devonian|Silurian|part of Amarra Suite||||||
21660|Dillons Knob Granite|69592|5|Briefly described|p293|Middle Devonian|Early Devonian|Lolworth Batholith, Charters Towers Province. Crops out over ~145 km2; forms numerous small knolls. Similar to Amarra Granite.||Amarra Suite.||||
21673|Djungan Volcanic Subgroup|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
21673|Djungan Volcanic Subgroup|23423|4|Described|p305 Table 7.3||Early Permian|Age: 281 +/- 2 Ma (Rb-Sr), ~280 Ma (Rb-Sr).  Featherbed Volcanic Group.||||||
21673|Djungan Volcanic Subgroup|23501|6|Mentioned|map legend|Early Permian|Early Permian|Of Featherbed Volcanic Group & Lags Supersuite.||||||
21673|Djungan Volcanic Subgroup|23616|5|Briefly described|Table 3 p46||Permian|Age: 281+/-2 Ma (Rb-Sr). Apparently unconformably overlies Fisherman Rhyolite; locally overlain by units of the Wakara Volcanic Subgp; intruded by microgranite plutons of  Lags Supersuite. Of Featherbed Volcanic Gp. Hodgkinson Province. Thickness ~2000 m.||||||
21673|Djungan Volcanic Subgroup|23713|5|Briefly described|p19||Early Permian|||||||
21673|Djungan Volcanic Subgroup|43087|5|Briefly described|p101|||Of Featherbed Volcanic Group.||||||
21673|Djungan Volcanic Subgroup|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Featherbed Volcanic Group||||||15-JUN-06
21673|Djungan Volcanic Subgroup|43254|5|Briefly described|map legend||Early Permian|of Featherbed Volcanic Group.||||||
21673|Djungan Volcanic Subgroup|43259|6|Mentioned|Appendix 1,p11.||Early Permian|||||||
21673|Djungan Volcanic Subgroup|43285|5|Briefly described|Map Legend||Permian|||||||
21673|Djungan Volcanic Subgroup|43626|2|Defined|p58|||||||||
21673|Djungan Volcanic Subgroup|44246|5|Briefly described|Map Legend||Early Permian|||||||
21673|Djungan Volcanic Subgroup|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Featherbed Volcanic Group. Geological Province: Kennedy Province.||||||
21673|Djungan Volcanic Subgroup|60425|3|Fully described|p45 Tb. 3, p46 Tb. 3|Early Permian|Early Permian|Of Featherbed Volcanic Gp. Locally overlain by Gavin Rhyolite (Wakara Volcanic Gp); unconformably overlies Fisherman Rhyolite; intruded by Bustlem Microgranite. Age: 281+/-2Ma, 280Ma (Rb-Sr). Thickness: >750m. Rhyolitic ignimbrite - detailed lith. given||||||07-FEB-11
21673|Djungan Volcanic Subgroup|62523|5|Briefly described|Map legend at p3-4|Early Permian|Early Permian|Of the Featherbed Volcanic Group, previously part of "Featherbed Volcanics". Represents one of the subsidence structures within the Featherbed Cauldron Complex. See also map and legend at p3-4.||||||07-FEB-11
21673|Djungan Volcanic Subgroup|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.||Unit in Featherbed Volcanic Group.|Includes Lightning Creek and Lumma Rhyolites.|||
21673|Djungan Volcanic Subgroup|69593|5|Briefly described|p484|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||Featherbed Volcanic Group.|||A-type.|
21699|Duck Granodiorite|23283|2|Defined|p24|Devonian|Silurian|||||||
21699|Duck Granodiorite|23505|5|Briefly described|Map legend|Devonian|Silurian|of Amarra Supersuite.||||||
21722|Earlscliffe Dacite|22675|4|Described|p47|Late Carboniferous|Late Carboniferous|Bulgonunna Volcanic Group||||||
21722|Earlscliffe Dacite|23161|5|Briefly described|p17 table3|Early Permian|Late Carboniferous|||||||
21722|Earlscliffe Dacite|43259|6|Mentioned|Appendix 1,p7.|Early Permian|Late Carboniferous|||||||
21722|Earlscliffe Dacite|43391|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the Bulgonunna Volcanic Group.  Grey crystal-rich to very crystal-rich rhyolitic ignimbrite.||||||23-JUN-04
21722|Earlscliffe Dacite|60659|5|Briefly described|p15|||Part of the Earscliffe association. Dark grey, crystal-rich to very crystal-rich dacitic ignimbrite intruded by voluminous rhyolite and quartz-feldspar porphyry. Intruded by Easter Granodiorite. Of the Bulgonunna Province.||||||07-FEB-11
21722|Earlscliffe Dacite|68679|5|Briefly described|p362|Permian|Permian|Kennedy Igneous Association. Early Pemian.|292.3 +/- 2.2 Ma (SHRIMP U-Pb: Cross et al., 2012)|Bulgonunna Volcanic Group.||||
21722|Earlscliffe Dacite|68901|5|Briefly described|p5, p117-p122, p145|Sakmarian|Sakmarian|Kennedy Igneous Association, Thomson Region. SHRIMP age is interpreted as the age of magmatic crystallisation. SHRIMP results and analysis discussed in detail.This unit can no longer be considered to represent the lowermost deposits of the Bulgonunna Volcanic Group.|292.3 +/- 2.2 Ma  (SHRIMP U-Pb)|Bulgonunna Volcanic Group|||Dated sample: Crystal-rich and densely welded rhyolitic ignimbrite.|16-NOV-18
21722|Earlscliffe Dacite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
21722|Earlscliffe Dacite|70740|5|Briefly described|p8, p82 fig 50, p87, p88, p111, p123|Early Permian|Early Permian|SHRIMP age derived from Cross et al, 2012. Appears as Earlscliff Ignimbrite on p8. Distinguished in radiometric images by dark pink tones. On the basis of radiometric images and air photos a number of informal subunits are interpreted.|292.3 +/- 2.2 Ma (SHRIMP U-Pb)|Bulgonunna Volcanic Group||Overlies the Ukalunda Formation. Probably overlain by the Collins Creek Rhyolite and Bobby Dazzler Rhyolite. Probably intruded by Perch Creek Granodiorite.|Grey, crystal-rich to very crystal-rich and lithic rich rhyolitic to dacitic ignimbrite.|
21726|Easter Granodiorite|22675|5|Briefly described|p112|Early Permian|Late Carboniferous|Drummond Basin||||||
21726|Easter Granodiorite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 230. I-Type.||||||
21726|Easter Granodiorite|43259|4|Described|Appendix 1,p32.|Permian|Carboniferous|U-Pb zircon age is 292+/-4 Ma.||||||
21726|Easter Granodiorite|43391|5|Briefly described|Map legend|Early Permian|Early Permian|Fine to medium hornblende-biotite granodiorite.||||||23-JUN-04
21726|Easter Granodiorite|43734|6|Mentioned|p10|||U-Pb age: 289.6+/-6.1 Ma||||||
21726|Easter Granodiorite|60659|5|Briefly described|p18|Early Permian|Late Carboniferous|Pale grey, fine- to medium-equigranular hornblende-biotite granodiorite.||||||07-FEB-11
21726|Easter Granodiorite|68900|6|Mentioned|p4|Permian|Permian|Drummond Basin.||||||
21726|Easter Granodiorite|69593|5|Briefly described|p495, p513|Permian|Late Carboniferous|Burdekin Falls Subprovince. Appears as Eastern in a list of granodiorites on p495. Sm-Nd isotope data tabulated.|290 +/- 6 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
21726|Easter Granodiorite|70740|5|Briefly described|p8, p123, p125|Sakmarian|Sakmarian|SHRIMP age derived from Black (1994). Distribution and geophysical and outcrop characteristics briefly discussed on p125.|289.6 +/- 6.1 (SHRIMP U-Pb)|||Probably intrudes the Easter Granodiorite.|Pale grey, fine to medium-grained, equigranular sphene bearing, hornblende-biotite granodiorite.|
21726|Easter Granodiorite|71592|5|Briefly described|Appendix A.|||Drummond Basin.|290+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
21737|Elbow Creek Granodiorite|22847|3|Fully described|p 41|||||||||
21737|Elbow Creek Granodiorite|23504|5|Briefly described|Map Legend||Ordovician|||||||
21737|Elbow Creek Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 492. I-Type.||||||
21737|Elbow Creek Granodiorite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Early to Middle Ordovician||||||
21737|Elbow Creek Granodiorite|43259|4|Described|Appendix 1,p51.||Ordovician|Ordovician?||||||10-FEB-09
21737|Elbow Creek Granodiorite|43936|5|Briefly described|Map Legend||Ordovician|||||||
21737|Elbow Creek Granodiorite|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Grey, medium-grained, porphyritic, hornblende-biotite granodiorite, minor monzogranite.||||||28-SEP-12
21737|Elbow Creek Granodiorite|70740|5|Briefly described|p39-p40|Ordovician|Ordovician|Outcrop characteristics discussed. A type area is mentioned and described. Ordovician age is tentative. Intruded by a number of unnamed gabbro and diorite plugs.|||||Grey, medium-grained and porphyritic hornblende-biotite granodiorite.|
21738|Election Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Supersuite.||||||
21738|Election Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21738|Election Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 430. I-Type.||||||
21738|Election Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
21738|Election Granite|43083|5|Briefly described|p254|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
21738|Election Granite|43087|2|Defined|p73|Late Carboniferous||Of Ootann Supersuite||||||
21738|Election Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21738|Election Granite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
21738|Election Granite|60425|4|Described|p278-9 Appdx|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). I-type. Medium- to fine-grained, highly porphyritic biotite granite; and fine-gr. (muscovite-) hornblende-biotite leucogranite with miarolitic cavities - with traces of late or post-magmatic fluorite.||||||07-FEB-11
21738|Election Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. The two main lithologies, as well as a geophysical subdivision described as a probable variant of the biotite granite, are mapped separately.||Unit in Ootann Supersuite.|||Medium- to fine-grained, highly porphyritic biotite granite; fine-grained (muscovite-) hornblende-biotite leucogranite with miarolitic cavities, extensively recrystallised with traces of late or post-magmatic fluorite.|
21752|Eridge Volcanic Member|23422|5|Briefly described|p205 Table 6.3|Early Carboniferous|Early Carboniferous|Of Tareela Volcanics, Glenrock Group.||||||
21752|Eridge Volcanic Member|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group.||||||
21752|Eridge Volcanic Member|43095|6|Mentioned|p22|||same as Eridge Member of Tareela Volcanics||||||
21752|Eridge Volcanic Member|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin. Subdivided into 4 unnamed units.||Of the Tareela Volcanics.||Conformably underlain by the Ponto Basalt Member.|Dacitic ignimbrite, dacitic lapilli tuff and breccia; rhyolitic ignimbrite and minor spherulitic rhyolite; dacitic to andesitic ignimbrite and tuff; rhyolitic to dacitic ignimbrite and minor tuff and volcanic siltstone.|
21752|Eridge Volcanic Member|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin. Informally subdivided into 4 unnamed units.||Of the Tareela Volcanics.||Conformably underlain by the Ponto Basalt Member.|Lithic-rich dacitic ignimbrite, dacitic lapilli tuff and breccia; rhyolitic ignimbrite and minor spherulitic rhyolite; dacitic to andesitic ignimbrite and tuff; crystal- and clast-rich rhyolitic to dacitic ignimbrite, minor tuff, volcanic siltstone.|
21789|Fish Creek Granite|23420|5|Briefly described|p 152 table 4.8||Early Devonian|In the Fish Creek Suite of the Kintore Supersuite||||||
21789|Fish Creek Granite|23496|5|Briefly described|Table 2, p41|Devonian|Silurian|of Fish Creek Suite, Kintore Supersuite.Inferred to intrude Rosser Schist and the Aralba and Laia Granites.||||||
21789|Fish Creek Granite|43287|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Fish Creek Suite.||||||
21789|Fish Creek Granite|43596|4|Described|p33, p28 Tb. 3|||Pale grey to brown (weathered) medium-grained, slightly porphyritic (garnet-) biotite-muscovite granite with sparse K-feldspar and muscovite phenocrysts.  Unassigned granite.||||||15-JAN-09
21789|Fish Creek Granite|69592|6|Mentioned|p282, p287 Fig.4.81|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
21791|Fisherman Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Yongala Volcanic Subgroup of Featherbed Volcanic Group.||||||
21791|Fisherman Rhyolite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup.||||||
21791|Fisherman Rhyolite|23501|5|Briefly described|map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup and Lags Supersuite.||||||
21791|Fisherman Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V111. A-Type.||||||
21791|Fisherman Rhyolite|23616|5|Briefly described|Table 3 p47||Permian|Of Yongala Volcanic Subgroup/Featherbed Volcanic Group.||||||
21791|Fisherman Rhyolite|23713|5|Briefly described|p22|||||||||
21791|Fisherman Rhyolite|43087|5|Briefly described|p83|||Of Featherbed Volcanic Group.||||||
21791|Fisherman Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21791|Fisherman Rhyolite|43254|5|Briefly described|map legend||Early Permian|Of Yongala Volcanic Subgroup.||||||19-FEB-07
21791|Fisherman Rhyolite|43259|4|Described|Appendix 1,p11.||Early Permian|Of Yongala Volcanic Subgroup.||||||19-FEB-07
21791|Fisherman Rhyolite|43285|5|Briefly described|Map Legend||Permian|Of Featherbed Volcanic Subgroup.||||||19-FEB-07
21791|Fisherman Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
21791|Fisherman Rhyolite|43626|2|Defined|p43-48||Early Permian|This unit has not been isotopically dated. The age (Rb-Sr isochron age: 267+/-7 Ma)obtained by Black (1978) included samples from the Arringunna Rhyolite and possibly also the Combella Rhyolite as well as the Fisherman Rhyolite.||||||02-APR-15
21791|Fisherman Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
21791|Fisherman Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Yongala Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
21791|Fisherman Rhyolite|60425|5|Briefly described|p46 Tb. 3|Early Permian|Early Permian|Of the Yongala Volcanic Subgroup (Featherbed Volcanic Group). Has two informal subunits. Unconformably overlain by Djungan Volcanic Subgroup units. Possibly disconformably overlies Timber Top Volcanic Subgroup units.||||||07-FEB-11
21791|Fisherman Rhyolite|62523|4|Described|p3-4 (map/legend), p9-10|Early Permian|Early Permian|Of Yongala Volcanic Subgroup. Lower sequence of rhyolitic ignimbrite and lava flows. Overlies/faulted against Timber Top Volcanic Subgroup; faulted against Djungan Volcanic Subgroup.||||||07-FEB-11
21791|Fisherman Rhyolite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province. Two variants are mapped separately: an intensely welded rhyolitic ignimbrite, rheomorphic flow structures common, minor rhyolitic lava, rare vitric fine-ash tuff, vitrophyre; and a slightly porphyritic rhyolite (lava flows, rare domes), commonly flow-banded, autobrecciated, minor rhyolitic fine-ash vitric and crystal tuffs.|273 +/- 7 Ma (Rb-Sr, total rock).|Unit in Yongala Volcanic Subgroup.|||Moderately crystal-rich to crystal-poor rhyolitic ignimbrite and slightly porphyritic rhyolite and rhyolite breccia (lava flows, domes); minor tuff; rare volcanic sandstone and siltstone.|
21791|Fisherman Rhyolite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated. Included in Lags Supersuite.|285 Ma.|Featherbed Volcanic Group.||||
21835|Gavin Rhyolite|23423|5|Briefly described|p305 Table 7.3||Early Permian|Wakara Volcanic Subgroup of Featherbed Volcanic Group.||||||
21835|Gavin Rhyolite|23500|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup.||||||
21835|Gavin Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. 103. A-Type.||||||
21835|Gavin Rhyolite|23616|5|Briefly described|Table 3 p46||Permian|Of Wakara Volcanic Subgroup. Hodgkinson Province.||||||
21835|Gavin Rhyolite|23713|5|Briefly described|p57 Plate 13|||Of Featherbed Volcanic Group.||||||
21835|Gavin Rhyolite|24485|6|Mentioned|p45|||||||||
21835|Gavin Rhyolite|24486|5|Briefly described|Map legend|Early Permian|Early Permian|Of the Wakara Volcanics Subgroup (Featherbed Volcanics Group).  Geological Province: Kennedy Province.||||||
21835|Gavin Rhyolite|43151|5|Briefly described|Map legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21835|Gavin Rhyolite|43254|5|Briefly described|map legend||Early Permian|of Wakara Volcanic Subgroup.||||||
21835|Gavin Rhyolite|43259|4|Described|Appendix 1,p10.||Early Permian|Of Wakara Volcanic Subgroup.||||||03-JUN-09
21835|Gavin Rhyolite|43567|5|Briefly described|Table 1,p399|||||||||
21835|Gavin Rhyolite|43625|5|Briefly described|p38|||||||||
21835|Gavin Rhyolite|43626|2|Defined|p81||Early Permian|Age between 289+/-10 Ma and 278+/-3 Ma.||||||03-JUN-09
21835|Gavin Rhyolite|44246|5|Briefly described|Map Legend||Early Permian|||||||
21835|Gavin Rhyolite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Wakara Volcanic Subgroup (Featherbed Volcanic Group). Geological Province: Kennedy Province.||||||
21835|Gavin Rhyolite|60425|5|Briefly described|p44 Tb. 3|Early Permian|Early Permian|Informal subunit of Wakara Volcanic Subgroup (Fatherbed Volcanic Group). Locally overlies Djungan Volcanic Subgroup.||||||07-FEB-11
21842|Gibbs Granite|23423|6|Mentioned|p306 Table 7.3|||||||||
21842|Gibbs Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
21842|Gibbs Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 249. I-Type.||||||
21842|Gibbs Granite|23616|6|Mentioned|Table 3 p48|||||||||
21842|Gibbs Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21842|Gibbs Granite|43259|4|Described|Appendix 1,p33.||Late Carboniferous|||||||
21842|Gibbs Granite|43626|6|Mentioned|p11|||||||||
21842|Gibbs Granite|60425|4|Described|p49 Tb.3, p278-9 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Intruded Boonmoo Volcanic Subgroup. I-type. Pale grey to pinkish grey, very highly porphyritic hornblende?-biotite microgranite.||||||07-FEB-11
21868|Glenroy Mill Granodiorite|23049|3|Fully described|p13|Ordovician|Ordovician|||||||
21868|Glenroy Mill Granodiorite|23283|2|Defined|p26|Devonian|Silurian|||||||
21868|Glenroy Mill Granodiorite|23422|5|Briefly described|p212 Table 6.7|||||||||
21868|Glenroy Mill Granodiorite|23505|5|Briefly described|Map legend|Devonian|Ordovician|||||||
21875|Gobongo Metamorphics|22845|2|Defined|p7,12-14,24,32,5,77|Early Carboniferous|Late Devonian|Little (1993) mapped as Kurwongbah beds.   Intruded by Station Creek Granodiorite.||||||
21875|Gobongo Metamorphics|22846|6|Mentioned|p58|Carboniferous|Devonian|||||||
21875|Gobongo Metamorphics|23608|6|Mentioned|p54|||||||||
21875|Gobongo Metamorphics|43588|6|Mentioned|p30|Early Carboniferous|Late Devonian|||||||
21875|Gobongo Metamorphics|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
21875|Gobongo Metamorphics|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: North D'Aguilar Subprovince (Wandilla Province).||||||
21875|Gobongo Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek and Rocksberg Greenstones, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
21875|Gobongo Metamorphics|68679|5|Briefly described|p325-326, p328, p330, p332, p470|Mississippian|Late Devonian|Donchak et al. (1995); Tang (2003). Kilkivan-Manumbar area, North D'Aguilar Subprovince. Lower plate accretionary assemblage. A structurally coherent unit. Has lithological and structural similarities with Anderson Creek Phyllite. Is intruded by Rush Creek Granodiorite. Is correlated with Kurwongbah beds.||||Is overlain structurally by, and locally faulted against Mount Mia Serpentinite and Amamoor beds. Locally interlayered with Widgee Metamorphics. Is overlain unconformably by North Arm Volcanic Group.|Interlayered phyllite and siliceous quartz-mica schist; metasiltstone. Rare thin layers of mafic greenschist. White quartzose laminae impart conspicuous banding. Transitional epidote-blueschist facies metamorphism.|
21884|Goolha-Goolha Schist|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|Coen Metamorphic Group||||||12-JAN-05
21884|Goolha-Goolha Schist|22781|4|Described|p25|Proterozoic|Proterozoic|Coen Metamorphic Group||||||
21884|Goolha-Goolha Schist|23420|5|Briefly described|p 142 table 4.4|||In the north east part of the Coen Metamorphic Group||||||
21884|Goolha-Goolha Schist|69591|5|Briefly described|p78 Tb.2.6|||Savannah Province, Coen Inlier.||Coen Metamorphic Group.|||Sillimanite-muscovite schist, quartzite.|
21884|Goolha-Goolha Schist|71792|5|Briefly described|p5, p6|Mesoproterozoic|Mesoproterozoic|Savannah Province. Includes a quartzite lens on Mount White. Misspelt as Goolha Goolha Schist p3, Fig.3.||||||
21884|Goolha-Goolha Schist|71849|5|Briefly described|p8, p98, p195|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.||Is intruded by Lankelly Granite.||
21884|Goolha-Goolha Schist|71853|5|Briefly described|Map legend.|||||||In places gradational into Lochs Gneiss.||
21884|Goolha-Goolha Schist|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic|||Coen Metamorphic Group.|||Sillimanite-garnet-muscovite schist, with feldspar, actinolite locally; some interbedded thin- to medium-bedded quartzite.|
21934|Gypsy Pocket Granodiorite|22630|5|Briefly described|p37|||||||||
21934|Gypsy Pocket Granodiorite|22844|6|Mentioned|p37|Permian|Carboniferous|||||||
21934|Gypsy Pocket Granodiorite|23049|3|Fully described|p66|||Probably Carboniferous or Permian in age.||||||
21934|Gypsy Pocket Granodiorite|23283|2|Defined|p29|Permian|Carboniferous|||||||
21934|Gypsy Pocket Granodiorite|23499|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
21938|Halpin Granite|23423|6|Mentioned|p306 Table 7.3|||||||||
21938|Halpin Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21938|Halpin Granite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite.||||||
21938|Halpin Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 248. I-Type.||||||
21938|Halpin Granite|23616|6|Mentioned|Table 3 p48|||||||||
21938|Halpin Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||15-JUN-06
21938|Halpin Granite|43259|4|Described|Appendix 1,p33.||Late Carboniferous|||||||
21938|Halpin Granite|43567|5|Briefly described|Table 2,p401|||||||||
21938|Halpin Granite|43626|6|Mentioned|p11|||||||||
21938|Halpin Granite|60425|5|Briefly described|p49 Tb.3, p278-9 Appdx. |Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite). Intruded Boonmoo Volcanic Subgroup. I-type. Pinkish grey to greenish grey, highly porphyritic biotite microgranite.||||||07-FEB-11
21938|Halpin Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pinkish grey to greenish grey, highly porphyritic biotite microgranite.|
21962|Hiker Granodiorite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Almaden Supersuite.||||||
21962|Hiker Granodiorite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Age: ~300 Ma, Rb-Sr. Of Almaden Supersuite.||||||31-MAR-15
21962|Hiker Granodiorite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 440. I-Type.||||||
21962|Hiker Granodiorite|23616|6|Mentioned|p71 Fig 13|||Of Almaden Supersuite.||||||
21962|Hiker Granodiorite|43060|5|Briefly described|Table 6|||of Almaden Supersuite||||||
21962|Hiker Granodiorite|43083|4|Described|p252|||Of Almaden Supersuite. I-type. Lithology included.||||||31-MAR-15
21962|Hiker Granodiorite|43087|2|Defined|p54|Late Carboniferous||||||||
21962|Hiker Granodiorite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite).||||||15-JUN-06
21962|Hiker Granodiorite|43259|4|Described|Appendix 1,p47.||Carboniferous|||||||
21962|Hiker Granodiorite|60425|4|Described|p280-1 Appdx. |Late Carboniferous|Late Carboniferous|Of Almaden Suite (Almaden Supersuite). Age: ~300Ma. I-type. Fine- to med.gr., variably porphyritic and heterogeneous (augite-) biotite-hornblende granodiorite + biotite-hornblende granodiorite; numerous mafic enclaves to ~10cm; gold-bearing veins, etc.||||||07-FEB-11
21962|Hiker Granodiorite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Almaden Supersuite.|||Medium to dark grey, fine- to medium-grained, variably porphyritic and heterogenous (augite)-biotite-hornblende granodiorite and biotite-hornblende granodiorite; with numerous mafic enclaves to ~10 cm.|
21969|Hogg Granodiorite|23032|5|Briefly described|p41|||||||||
21969|Hogg Granodiorite|23422|5|Briefly described|p215 Table 6.9|||||||||
21969|Hogg Granodiorite|23499|5|Briefly described|map legend|Devonian|Silurian|Reedy Springs Batholith.||||||
21969|Hogg Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
21969|Hogg Granodiorite|43480|2|Defined|7-36|Devonian|Silurian|||||||
21969|Hogg Granodiorite|64707|5|Briefly described|Map legend|Early Devonian|Silurian|Intensely foliated buff to grey, medium- to coarse-grained, subequigranular garnet-biotite-muscovite granodiorite.||||||08-MAY-15
21969|Hogg Granodiorite|68338|5|Briefly described|Map legend.|Early Devonian|Silurian|Unit in Reedy Springs Batholith, Pama Province.|||||Intensely foliated buff to grey medium- to coarse-grained, subequigranular garnet-biotite-muscovite granodiorite.|
21969|Hogg Granodiorite|69592|5|Briefly described|p284|||Reedy Springs Batholith, Charters Towers Province.||Upland Supersuite.|||I-type.|
21977|Hopscotch Rhyolite|23423|5|Briefly described|p306 Table 7.3||Late Carboniferous|Boonmoo Volcanic Subgroup of Featherbed Volcanic Group.||||||
21977|Hopscotch Rhyolite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Boonmoo Volcanic Subgroup.||||||
21977|Hopscotch Rhyolite|23506|5|Briefly described|Map Legend||Late Carboniferous|of Boonmoo Volcanic Subgroup, Featherbed Volcanic Group.||||||
21977|Hopscotch Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V130. I-Type.||||||
21977|Hopscotch Rhyolite|23616|5|Briefly described|Table 3 p49|||Of Boonmoo Volcanic Subgroup||||||
21977|Hopscotch Rhyolite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||15-JUN-06
21977|Hopscotch Rhyolite|43259|4|Described|Appendix 1,p14.||Carboniferous|of Boonmoo Volcanic Subgroup.||||||
21977|Hopscotch Rhyolite|43567|5|Briefly described|Table 2,p400|||||||||
21977|Hopscotch Rhyolite|43626|2|Defined|p24|||between 306+/-3 Ma and 304+/-4 Ma||||||
21977|Hopscotch Rhyolite|44246|5|Briefly described|Map Legend||Late Carboniferous|||||||
21977|Hopscotch Rhyolite|60425|5|Briefly described|p48 Tb. 3|||Of the Boonmoo Volcanic Subgroup (Featherbed Volcanic Group).||||||07-FEB-11
21977|Hopscotch Rhyolite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Two un-named "geophysical subdivisions" are mapped separately: one with relatively high magnetic response and the other with purplish tones on the composite radiometric image.||Unit in Boonmoo Volcanic Subgroup.|||Medium to dark or greenish grey, moderately to intensely welded, lithics-poor to lithics-free, crystal-rich, hornblende-biotite rhyodacitic ignimbrite; with fiamme up to 10 cm x 2 cm; very coarse, crystal-rich rhyodacitic ignimbrite.|
21977|Hopscotch Rhyolite|68576|5|Briefly described|Q_11: p11||||308+/- 8 Ma (Rb-Sr total rock isochron age).|Boonmoo Volcanic Subgroup.||Overlies Muirson Rhyolite.||
21979|House and Kitchen Granite|22675|4|Described|p157 App.1|Late Carboniferous|Late Carboniferous|||||||
21979|House and Kitchen Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 231. I-Type.||||||
21979|House and Kitchen Granite|43391|5|Briefly described|Map legend|Carboniferous|Carboniferous|?Early Carboniferous.  Aphyric to sparsely porphyritic very fine granite.||||||23-JUN-04
21979|House and Kitchen Granite|60659|5|Briefly described|p18|||Mid-pink to pale red equigranular to sparsely porphyritic microgranite to a very fine-grained granite.||||||07-FEB-11
21979|House and Kitchen Granite|68900|6|Mentioned|p4|Carboniferous|Carboniferous|Drummond Basin.||||||
21979|House and Kitchen Granite|70740|5|Briefly described|p84, p120, p126|||||||Intrudes the Hidden Valley Rhyolite, Ukalunda Formation.|Pink to pale red, equigranular to sparsely porphyritic microgranite to very fine-grained aplitic granite. Porphyritic, graphic syenogranite also observed.|
21997|Indicator Granite|23423|6|Mentioned|p307 Table 7.3|||||||||
21997|Indicator Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|Ootann Supersuite.||||||
21997|Indicator Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 327. I-Type.||||||
21997|Indicator Granite|43151|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).||||||03-JUN-09
21997|Indicator Granite|43259|4|Described|Appendix 1,p39.||Carboniferous|Late? Carboniferous in age.||||||
21997|Indicator Granite|60425|5|Briefly described|p47 Tb. 3, p278-9 Appdx.|Late Carboniferous|Late Carboniferous|Cuts the Boxwood Volcanics (Featherbed Volcanic Group). I-type. Pink, medium-grained, slightly porphyritic biotite-hornblende granite.||||||07-FEB-11
21997|Indicator Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in Ootann Supersuite.|||Pink to grey, medium-grained, slightly porphyritic hornblende-biotite monzogranite.|
21999|Ingleby Granite|23420|4|Described|p 150 table 4.8||Early Devonian|In the Ebagoola Suite of the Kintore Supersuite. Intrudes Holroyd Group||||||
21999|Ingleby Granite|43596|5|Briefly described|p26 Tb. 2, p27 Tb. 3, p35|||Of Ebagoola Suite (Kintore Supersuite).  Intrudes Dinah Formation and Sugrabag Creek Quartzite. Pale grey to buff, equigranular muscovite-biotite granite (musc.-poor) with rare K-feldspar phenocrysts and local microdiorite enclaves; garnet-musc. leucogranite; pegmatite, quartz.||||||07-APR-15
21999|Ingleby Granite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Kintore Supersuite.||||
10002|Lady Loretta Formation|22438|4|Described|p539, Fig.3 p537|||Youngest unit in Fiery Creek Dome region. See also Fig.10a p546||||||
10002|Lady Loretta Formation|22453|5|Briefly described|p 11  Fig 10|||||||||
10002|Lady Loretta Formation|22585|6|Mentioned|P739, Fig2, Fig3|||||||||
10002|Lady Loretta Formation|22680|6|Mentioned|83,85,87|||||||||
10002|Lady Loretta Formation|22681|5|Briefly described|89,90|Proterozoic|Proterozoic|Max thickness 2000 m. Underlain by Esperanza Formation.||||||09-OCT-06
10002|Lady Loretta Formation|23031|3|Fully described|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Shady Bore Quartzite.||||||09-OCT-06
10002|Lady Loretta Formation|23072|5|Briefly described|p754|||||||||
10002|Lady Loretta Formation|23362|5|Briefly described|339|||||||||
10002|Lady Loretta Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|||||||
10002|Lady Loretta Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
10002|Lady Loretta Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies the Esperanza Formation ; underlies Shady Bore Quartzite.||||||07-NOV-08
10002|Lady Loretta Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23397|5|Briefly described|p469|||||||||
10002|Lady Loretta Formation|23398|4|Described|p449|Statherian|Statherian|Of McNamara Group.  Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23399|5|Briefly described|p503|||Of McNamara Group..||||||09-OCT-06
10002|Lady Loretta Formation|23406|5|Briefly described|p606, p612|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4Ma. Geological province: Lawn Hill Platform. Contains a basal breccia layer.||||||16-JUN-09
10002|Lady Loretta Formation|23408|5|Briefly described|p511, p513 Fig. 2, p523|||Of McNamara Group. Includes a basal breccia which is interpreted to form the basal unconformity of the Lady Loretta Supersequence.||||||15-JUN-09
10002|Lady Loretta Formation|23409|4|Described|p539 Tab.1|Statherian|Statherian|Age: 1647+/-4Ma.||||||09-OCT-06
10002|Lady Loretta Formation|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
10002|Lady Loretta Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
10002|Lady Loretta Formation|23958|5|Briefly described|p1134|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
10002|Lady Loretta Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 2000m.||||||
10002|Lady Loretta Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
10002|Lady Loretta Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
10002|Lady Loretta Formation|24309|5|Briefly described|p1018|Proterozoic|Proterozoic|Of the McNamara Group.||||||09-OCT-06
10002|Lady Loretta Formation|24432|4|Described|p560 Tb.1, p562 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1647+/-4 Ma. Carbonaceous, pyritic, dolomitic and sideritic siltstone and shale. Geological Province: Lawn Hill Platform.||||||
10002|Lady Loretta Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|36937|6|Mentioned|p229|||||||||
10002|Lady Loretta Formation|37459|1|Redefined|p430|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
10002|Lady Loretta Formation|37568|6|Mentioned|p84|||||||||
10002|Lady Loretta Formation|37569|6|Mentioned|p93|||||||||
10002|Lady Loretta Formation|38237|4|Described|p129|||||||||
10002|Lady Loretta Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|38348|4|Described|p12|||||||||
10002|Lady Loretta Formation|38584|6|Mentioned|p22|||||||||
10002|Lady Loretta Formation|39445|5|Briefly described|Table 2|||||||||
10002|Lady Loretta Formation|39497|6|Mentioned|Fig.4|||||||||
10002|Lady Loretta Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.||||||15-JUN-06
10002|Lady Loretta Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|39925|6|Mentioned|Fig.9|||||||||
10002|Lady Loretta Formation|39943|6|Mentioned|Table 1A|||||||||
10002|Lady Loretta Formation|39944|6|Mentioned|p228|||||||||
10002|Lady Loretta Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10002|Lady Loretta Formation|40179|5|Briefly described|p306|||||||||
10002|Lady Loretta Formation|40221|3|Fully described|p18|||||||||
10002|Lady Loretta Formation|40394|6|Mentioned|Fig.2|||||||||
10002|Lady Loretta Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
10002|Lady Loretta Formation|42166|6|Mentioned|p111|||||||||
10002|Lady Loretta Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||09-OCT-06
10002|Lady Loretta Formation|43615|6|Mentioned|p13|||||||||
10002|Lady Loretta Formation|45166|5|Briefly described|p30|||||||||
10002|Lady Loretta Formation|47083|3|Fully described|p17||Proterozoic|Previously part of Paradise Creek Formation of Carter and others (1961). Of McNamara Gp. Overlain by Shady Bore Quartzite; underlain by Esperanza Fm. Max thickness: 1800 m.||||||09-OCT-06
10002|Lady Loretta Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1647 Ma, <1657 Ma. Conformably overlies Esperanze Formation, conformably overlain by Shady Bore Quartzite. Geological Province: Western Fold Belt.||||||17-DEC-07
10002|Lady Loretta Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Laminated and massive dolomite; intraclastic, oolitic and stromatolitic dolomite; ferruginous chert breccia, flaggy siltstone and fine sandstone.  Overlies Esperanza Formation; overlain by Shady Bore Quartzite.||||||28-JUN-04
10002|Lady Loretta Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Shady Bore Quartzite, underlain by Esperanza Formation.||||||
10002|Lady Loretta Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
10002|Lady Loretta Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Hosts Lady Loretta deposit (Zn-Pb-Ag stratiform). Shown as Lady Loretta Fm.||McNamara Group|||Platform carbonates.|
10002|Lady Loretta Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1647 +/- 4 Ma.|McNamara Group.||||
10002|Lady Loretta Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
10002|Lady Loretta Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
10002|Lady Loretta Formation|63113|6|Mentioned|p1214,1219,1220,1225: Figs.2,8,9,13. |||Part of Loretta supersequence.|1647 Ma.|Of the McNamara Group||Is overlain by Riversleigh Siltstone or ?unconformably by Shady Bore Quartzite.||
10002|Lady Loretta Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Loretta supersequence||Is overlain by Shady Bore Quartzite.||
10002|Lady Loretta Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
10002|Lady Loretta Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
10002|Lady Loretta Formation|63866|5|Briefly described|p57|Statherian|Statherian|Isa Superbasin.|1647 +/- 4 Ma|Loretta Supersequence||||
10002|Lady Loretta Formation|64250|6|Mentioned|p11 fig 3||||1647 +/- 4 Ma|Unit in McNamara Group.||||
10002|Lady Loretta Formation|64575|6|Mentioned|p665|||||||||
10002|Lady Loretta Formation|65228|5|Briefly described|p26, Fig.04.|Statherian|Statherian|Part of Loretta Supersequence.|1647 +/- 4 Ma (SHRIMP).|||Equivalent to Loretta Supersequence.||
10002|Lady Loretta Formation|65337|6|Mentioned|p33 Fig.27.|||Correlates with upper Brumby Formation.||||Overlies Esperanza Formation. Is overlain by Shady Bore Quartzite.||
10002|Lady Loretta Formation|65396|5|Briefly described|p82, p175, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform. Detrital zircon sources listed.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation; overlain by Shady Bore Quartzite.||03-APR-17
10002|Lady Loretta Formation|66844|5|Briefly described|p245,268, 269|Mesoproterozoic|Statherian|Lawn Hill and Gunpowder region. Age from SHRIMP dating.|1647+\-3 Ma|Within Loretta Supersequence.||Underlain unconformably by Esperanza Formation. Overlain by upper McNamara Group.|Basal breccia, marine carbonates and siliciclastics.|
10002|Lady Loretta Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p60|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|1647 +/- 4 Ma (maximum depositional age).|McNamara Group.|||Laminated stromatolitic and intraclastic dolomite, dolomitic siltstone, limestone, shale|
10002|Lady Loretta Formation|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlies Esperanza Formation||
10002|Lady Loretta Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier. Hosts the exceptionally high-grade, sediment-hosted Lady Loretta Zn-Pb-Ag deposit (described in detail).||Lower McNamara Group.|||Basal interbedded dolomitic siltstone and sandstone; then interbedded pyrite, argillaceous siltstone and minor sandstone; banded to massive sulfides, locally baritic; massive siltstone locally pyritic; interbedded siltstone, sandstone and sulfides.|
10002|Lady Loretta Formation|68732|5|Briefly described|p162, p165 Fig.3|Statherian|Statherian|Of the Loretta Supersequence. Sedimentary depositional age.|1647 +/- 4 Ma|Of the McNamara Group.||||
10002|Lady Loretta Formation|69591|4|Described|p42, p43-44, p54|||Isa Superbasin. Thins to the NNW. Deposited on a shallow carbonate platform: subtidal/inner shelf/outer ramp deposits. Loretta Supersequence.|~1647 Ma (Betts et al., 1999).|McNamara Group.||Overlies Esperanza Formation.|Laminated stromatolitic and intraclastic dolomite, dolomitic siltstone, limestone, shale.|
10002|Lady Loretta Formation|70864|5|Briefly described|p75, 74 Fig 2, p78, p80, 81, 84, 100|Mesoproterozoic||||McNamara Group|||Stromatolitic dolostones, dolomitic siltstone and carbonaceous pyritic shale.|
10002|Lady Loretta Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1648+/-13 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuffite or shale.|
10002|Lady Loretta Formation|72526|5|Briefly described|p1, p8 Fig.1.3, p10, p85.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age based on the age of tuffaceous intervals (Page and Sweet, 1998; Page et al., 2000; Carson et al., 2011b). Age given as U-Pb zircon sedimentary depositional age.|1647 +/-4 Ma.|McNamara Group||Overlies Esperanza Formation and conformably underlies Shady Bore Quartzite.||
10002|Lady Loretta Formation|72912|4|Described|p5 Fig.3, p15, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional age [?] given.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation and underlies Shady Bore Quartzite.|Includes dolomitic siltstone.|
10002|Lady Loretta Formation|72913|5|Briefly described|p4,p7,  p8, p9 Tb.1, p22, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in Argyle Creek 1 in this study.  Mineral composition shows majority quartz and dolomite.|1647 +/- 4 Ma|McNamara Group||Overlies Esperanza Formation and underlies Shady Bore Quartzite.|Includes dolomitic siltstone.|
10002|Lady Loretta Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
10002|Lady Loretta Formation|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1647 +/- 4 Ma (see Fig.1.2)|McNamara Group||Underlain by Esperanza Formation. Overlain by Shady Bore Quartzite unconformably in part.||
10002|Lady Loretta Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Loretta Supersequence. Aquifer. Includes oil show. Deposited in subtidal tempestite cycles (Southgate et al., 2000).||McNamara Group||Underlain by Esperanza Formation. Unconformably overlain by Riversleigh Siltstone.|Dolomudstone.|
10002|Lady Loretta Formation|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Carbonates.|
10010|Lags Supersuite|23076|4|Described|p724, 727|Early Permian|Early Permian|290-280 M yr.||||||
10010|Lags Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
10010|Lags Supersuite|23423|4|Described|p315 Table 7.4||Early Permian|Intrudes Featherbed Volcanic Group. Also see p243. Age: 279 +/- 4 Ma, 280 +/- 4 Ma (Rb-Sr).||||||
10010|Lags Supersuite|23500|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10010|Lags Supersuite|23501|6|Mentioned|map legend|Early Permian|Early Permian|||||||
10010|Lags Supersuite|23616|4|Described|Table 3 p46, p80||Early Permian|Age: ~280 Ma. Interpreted from constituent unit ages and surrounding units. Hodgkinson Province.||||||
10010|Lags Supersuite|23713|4|Described|p29||Early Permian|||||||
10010|Lags Supersuite|24485|5|Briefly described|p41, p48 Tb.8|Early Permian|Early Permian|Intrudes the Wakara Volcanic Subgroup||||||
10010|Lags Supersuite|24486|5|Briefly described|Map legend|Early Permian|Early Permian|||||||
10010|Lags Supersuite|42681|5|Briefly described|p21|||Reserved as Lags Microgranite.||||||
10010|Lags Supersuite|43060|4|Described|p112|||||||||
10010|Lags Supersuite|43083|4|Described|p131|Early Permian|Early Permian|Of Mckenzie et al (1993). Scattered dykes, lenses and small plutons.||||||17-JUN-09
10010|Lags Supersuite|43254|5|Briefly described|map legend||Early Permian|||||||
10010|Lags Supersuite|43285|5|Briefly described|Map Legend||Early Permian|||||||
10010|Lags Supersuite|43625|4|Described|p51|||||||||
10010|Lags Supersuite|44246|6|Mentioned|Map Legend||Early Permian|||||||
10010|Lags Supersuite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province.||||||
10010|Lags Supersuite|60425|3|Fully described|p58 Tb. 4, p77, p276-7 Appdx. |Early Permian|Early Permian|Contains Lags and Maneater Suites + unassigned Bustlem Microgranite + Saint Helena Monzogranite. Supersuite age: 279+/-4Ma, 280+/-4Ma. A-type, highly porphyritic to even-grained microgranite to microgranodiorite; minor microdiorite, dacite (intrusive).||||||07-FEB-11
10010|Lags Supersuite|62371|5|Briefly described|p472 Fig.3|Permian|Carboniferous|A-type.||||||
10010|Lags Supersuite|63140|6|Mentioned|p572 fig 3|Early Permian|Early Permian||||||A-type.|
10010|Lags Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province. Granites are A-type.||||||
10010|Lags Supersuite|68337|5|Briefly described|Map legend|Early Permian|Early Permian|Kennedy Province.|||Includes Maneater Granodiorite, Saint Helena Monzogranite and Lags Microgranite.|||
10010|Lags Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Brodies Camp, Pieter Botte, Weymouth, Whypalla, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
10010|Lags Supersuite|69030|5|Briefly described|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.|279 +/- 4 Ma (Rb/Sr isochron age).||||A-type granitoids.|
10010|Lags Supersuite|69593|4|Described|p484-485, p487-488, p503-504, p510|Permian|Permian|Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Confined to small high-level plutons and dykes at the Featherbed Cauldron Complex. Geochemistry described. Early Permian.|~280 Ma (Rb-Sr).||Lags, Maneater Suites; Djungan, Wakara, Yongala, Volcanic Subgroups.||A-type. Generally strongly porphyritic, fayalite-pyroxene microgranite, hornblende microgranite, (hornblende-)biotite, and biotite microgranite, biotite-hornblende and biotite granodiorite, and minor quartz diorite; volcanics.|
10047|Lake Galilee Sandstone|13516|6|Mentioned|p147, fig 5|Carboniferous|Carboniferous|From Galilee Basin||||||
10047|Lake Galilee Sandstone|23430|4|Described|p519 Table 14.6|||Maximum thickness <260 m.||||||
10047|Lake Galilee Sandstone|30915|6|Mentioned|p100|||||||||
10047|Lake Galilee Sandstone|31120|6|Mentioned|p155|||||||||
10047|Lake Galilee Sandstone|31121|6|Mentioned|p385|||||||||
10047|Lake Galilee Sandstone|31122|2|Defined|p349|Early Permian|Late Carboniferous|Probably Late Carboniferous to Early Permian||||||
10047|Lake Galilee Sandstone|31258|4|Described|p98|||||||||
10047|Lake Galilee Sandstone|31860|6|Mentioned|p277|||See also P281||||||
10047|Lake Galilee Sandstone|33372|6|Mentioned|p16|||Re-strat.||||||
10047|Lake Galilee Sandstone|33674|4|Described|p438|||Lithology.||||||
10047|Lake Galilee Sandstone|35457|6|Mentioned|p627|||Also Fig.4 biostratigraphic relationships.||||||
10047|Lake Galilee Sandstone|35845|6|Mentioned|Fig.25|||||||||
10047|Lake Galilee Sandstone|36243|6|Mentioned|Table 5A|||||||||
10047|Lake Galilee Sandstone|36921|4|Described|p183|||See also Table 1.||||||
10047|Lake Galilee Sandstone|37451|6|Mentioned|Table 2|||||||||
10047|Lake Galilee Sandstone|37610|4|Described|p301|||See also Fig.3.||||||
10047|Lake Galilee Sandstone|39264|6|Mentioned|Fig.13|||||||||
10047|Lake Galilee Sandstone|39265|6|Mentioned|Fig. 3|||||||||
10047|Lake Galilee Sandstone|39445|5|Briefly described|Table 7|||See also p92.||||||20-SEP-18
10047|Lake Galilee Sandstone|39478|6|Mentioned|Table 1|||||||||
10047|Lake Galilee Sandstone|39847|6|Mentioned|p34|||||||||
10047|Lake Galilee Sandstone|39943|6|Mentioned|Table 7A|||||||||
10047|Lake Galilee Sandstone|39989|6|Mentioned|p426|||||||||
10047|Lake Galilee Sandstone|39991|6|Mentioned|p428|||||||||
10047|Lake Galilee Sandstone|40123|6|Mentioned|p465|||||||||
10047|Lake Galilee Sandstone|41116|5|Briefly described|p430|||||||||
10047|Lake Galilee Sandstone|41198|6|Mentioned|Table 1|||||||||
10047|Lake Galilee Sandstone|41707|6|Mentioned|Fig.8|||||||||
10047|Lake Galilee Sandstone|41710|6|Mentioned|p224|||||||||
10047|Lake Galilee Sandstone|42447|6|Mentioned|Fig.25b|||||||||
10047|Lake Galilee Sandstone|42547|5|Briefly described|p80|||||||||
10047|Lake Galilee Sandstone|42999|5|Briefly described|Table 1,p90||Late Carboniferous|||||||
10047|Lake Galilee Sandstone|43105|5|Briefly described|p13|||||||||
10047|Lake Galilee Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
10047|Lake Galilee Sandstone|46849|6|Mentioned|Fig. 7|||||||||
10047|Lake Galilee Sandstone|46881|6|Mentioned|Fig.7|||||||||
10047|Lake Galilee Sandstone|63713|5|Briefly described|p1507 Fig.2, p1508|Pennsylvanian|Pennsylvanian|Eastern margin, Galilee Basin.||Unit in Joe Joe Group.||Is overlain by Jericho Formation.||
10047|Lake Galilee Sandstone|63832|5|Briefly described|p134|Serpukhovian|Serpukhovian|Gray and Swarbrick (1975). Of Galilee Basin. Known from drillcores only; a complete nonglacial-glacial-nonglacial cycle. Second (C2) glaciation.|||||Contains complexly interbedded diamictites and other characteristic glacial facies.|13-DEC-17
10047|Lake Galilee Sandstone|64288|5|Briefly described|p532 Fig.1 |Serpukhovian|Serpukhovian|||Unit in Joe Joe Group.||Is overlain by Jericho Formation.||
10047|Lake Galilee Sandstone|64631|5|Briefly described|p47.|Bashkirian|Serpukhovian|Galilee Basin subsurface. See also p44. Some Serpukhovian biostratigraphic age control.||Of Joe Joe Group?|||Contains complexly interbedded diamictites and other characteristic glacial facies.|
10047|Lake Galilee Sandstone|65382|5|Briefly described|p714|Serpukhovian|Serpukhovian|Overlies Ducabrook Formation of the Drummond Basin. Age of 323 Ma given based on occurrence of the Spelaeotriletes ybertii Assemblage.||||||
10047|Lake Galilee Sandstone|65489|6|Mentioned|p144 Fig.53|Late Carboniferous|Late Carboniferous|Koburra Trough, Galilee Basin.||||||
10047|Lake Galilee Sandstone|66188|6|Mentioned|435, Fig 3,17|Early Permian|Late Carboniferous|Included in the Jericho Formation for the purposes of this study.||||||
10047|Lake Galilee Sandstone|67402|5|Briefly described|p124 fig GLL1, p125 tbl GLL1|Gzhelian|Kasimovian|Galilee Basin. Deposited in a braided fluvial environment. Sandstones generally have poor reservoir quality due to pressure solution, quartz cementation and kaolinite clay development. Approximately 200m thick.||||Overlain by the Jericho Formation.|Sub-labile to quartzose sandstones with minor mudstone.|
10047|Lake Galilee Sandstone|68731|5|Briefly described|p175, p198, p201 Fig 3.110|Pennsylvanian|Mississippian|Restricted to the Koburra Trough, and represents initiation of sedimentation during the Mississippian(?)/Pennsylvanian.||Of the Joe Joe Group.||||
10047|Lake Galilee Sandstone|69582|6|Mentioned|p65|Early Carboniferous|Early Carboniferous|Galilee Basin.||||Unconformably overlain by the Jericho Formation.|Siltstone.|
10047|Lake Galilee Sandstone|71265|5|Briefly described|p589|Bashkirian|Bashkirian|Eastern Galilee Basin.||||Is overlain by Jericho Formation.||
10047|Lake Galilee Sandstone|71701|5|Briefly described|p155-p156|Bashkirian|Bashkirian|Confined to the northernmost part of the Springsure Shelf and the Koburra Trough.||Joe Joe Group||Overlain by the Jericho Formation.||
10047|Lake Galilee Sandstone|71710|4|Described|p370, p374, p375 Fig 9, p384, p385|Late Carboniferous|Late Carboniferous|Geological province: Galilee Basin. Depositional environment, well log character and sequence stratigraphy described. Cratonic provenance. Local variations include sub-bituminous coal seam and carbonaceous band in upper section (Carmichael-1, Koburra-1) and conglomerate with clasts of quartz, quartzite, chert, rare shale and limestone (Koburra-1, Lake Galilee-1).||Unit of Joe Joe Group. With lower Jericho Formation, forms sequence 1, this paper.||Overlain by Jericho Formation. Unconformably overlies the Natal Formation of the Drummond Basin. Both upper and lower boundaries are sharp.|Fine to coarse-grained quartz lithic sandstone overlain by siltstone to claystone, overlain by interbedded, fine to medium-grained quartz-feldpathic sandstone and siltstone.|
10047|Lake Galilee Sandstone|72088|4|Described|p8, p17,|Serpukhovian|Serpukhovian|Eastern Galilee Basin, restricted to the Koburra Trough. Deposited by braided streams.||Joe Joe Group||Conformably overlain by the Jericho Formation.|Quartzose sandstone and minor conglomerate, mudstone and siltstone.|
10047|Lake Galilee Sandstone|72297|5|Briefly described|p747|||Koburra Trough, Galilee Basin. Two wells intersecting this unit have provided the only oil and gas shows in the Basin to date [2013]; porosity and permeability briefly discussed: unlikely to contain significant hydrocarbons.||||||
10047|Lake Galilee Sandstone|73163|5|Briefly described|p467|||Galilee Basin. Restricted to the Koburra Trough and eastern margin of the Galilee Basin.||Joe Joe Group||Conformably underlying the Jericho Formation.|Silicified, very fine- to medium-grained quartz sandstone.|
10047|Lake Galilee Sandstone|73472|6|Mentioned|p115|Serpukhovian|Serpukhovian|Galilee Basin.||Joe Joe Group||Overlain by Jericho Formation.||
10117|Lamington Group|23811|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Includes Lismore Basalt.||||||19-NOV-08
10117|Lamington Group|23812|5|Briefly described|p37 Tb.5|Tertiary|Tertiary|||||||
10117|Lamington Group|30687|5|Briefly described|p65|||Tertiary age||||||
10117|Lamington Group|31130|6|Mentioned|p932|||Tertiary||||||
10117|Lamington Group|31273|6|Mentioned|p24|||||||||
10117|Lamington Group|33290|6|Mentioned|p37|||||||||
10117|Lamington Group|33381|6|Mentioned|p108|||Tertiary.||||||
10117|Lamington Group|34755|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|35045|6|Mentioned|p110|||||||||
10117|Lamington Group|35050|6|Mentioned|p130|||||||||
10117|Lamington Group|35126|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|35156|4|Described|p7|||See also Table.2||||||
10117|Lamington Group|35296|6|Mentioned|p12|||Statigraphy.||||||
10117|Lamington Group|35866|6|Mentioned|p407|||||||||
10117|Lamington Group|36779|5|Briefly described|p8|||||||||
10117|Lamington Group|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|38080|6|Mentioned|p55|||||||||
10117|Lamington Group|38441|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|39445|6|Mentioned|Table 14|||||||||
10117|Lamington Group|39998|6|Mentioned|p190|||||||||
10117|Lamington Group|40623|5|Briefly described|p109|||||||||
10117|Lamington Group|40896|6|Mentioned|p49|||||||||
10117|Lamington Group|41906|3|Fully described|Table 4 P32|||||||||
10117|Lamington Group|43008|5|Briefly described|map legend|||||||||
10117|Lamington Group|44782|14|Not recorded|p44|||||||||
10117|Lamington Group|44783|14|Not recorded|p12,19|||||||||
10117|Lamington Group|44784|4|Described|p11,12||Tertiary|Includes: Hobwee Basalt, Binna Burra Rhyolite, Mount Lindsay Rhyolite, Chinghee Conglomerate, Hillview Rhyolite, Albert Basalt, Numinbah Valley Formation.||||||
10117|Lamington Group|44786|14|Not recorded|p193-202||Miocene|Early Miocene||||||
10117|Lamington Group|44813|14|Not recorded|p80-85,88||Tertiary|Apparent age: 22-20 Ma||||||
10117|Lamington Group|44818|6|Mentioned|p275|||||||||
10117|Lamington Group|61155|5|Briefly described|p19|Early Miocene|Early Miocene|Of the Main Range Volcanics. Associated with the Tweed Volcano. Overlies Numinbah Valley Formation. Age: 22-17Ma. In the Brisbane region.||||||
10117|Lamington Group|63779|6|Mentioned|p1140|Cenozoic|Cenozoic|Age: between 25 - 20Ma. Volcanics.||||||
10117|Lamington Group|68327|5|Briefly described|Map legend.|Tertiary|Tertiary|Three facies, labelled Ts, Tl and Tv, are mapped separately.|||||Ts = mudstone, siltstone, shale, sandstone, lenses of basalt; Tl = basalt flows, minor rhyolite and pyroclastics; Tv = mainly basalt flows.|
10117|Lamington Group|68553|6|Mentioned|Map legend|Paleogene|Paleogene|||||||
10120|Lamington Volcanics|22582|5|Briefly described|p69||Early Miocene|||||||
10120|Lamington Volcanics|23888|5|Briefly described|p262|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|24299|5|Briefly described|p4|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|30131|6|Mentioned|p8|||See also P11. Lithology||||||
10120|Lamington Volcanics|30604|6|Mentioned|p65|||||||||
10120|Lamington Volcanics|32491|6|Mentioned|p22|||||||||
10120|Lamington Volcanics|32492|6|Mentioned|Map legend|Miocene|Miocene|||||||
10120|Lamington Volcanics|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|33476|4|Described|p106|||||||||
10120|Lamington Volcanics|33766|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|35042|5|Briefly described|p129|||||||||
10120|Lamington Volcanics|35045|6|Mentioned|p110|||||||||
10120|Lamington Volcanics|35050|6|Mentioned|p130|||||||||
10120|Lamington Volcanics|35296|6|Mentioned|p12|||Statigraphy.||||||
10120|Lamington Volcanics|36806|6|Mentioned|p131|||||||||
10120|Lamington Volcanics|40328|6|Mentioned|p195|||||||||
10120|Lamington Volcanics|40896|6|Mentioned|p5|||||||||
10120|Lamington Volcanics|43150|5|Briefly described|Map Legend||Tertiary|||||||
10120|Lamington Volcanics|43881|14|Not recorded|p53||Tertiary|Equivalent to MacPherson Volcanics. Probably Eocene-Oligocene||||||
10120|Lamington Volcanics|44781|14|Not recorded|p355|||||||||
10120|Lamington Volcanics|44783|14|Not recorded|p2|||||||||
10120|Lamington Volcanics|48917|4|Described|p38|||See also P33. Stratigraphic table||||||
10120|Lamington Volcanics|60079|5|Briefly described|Map Legend|Tertiary|Tertiary|Includes: Lismore Basalt.||||||
10120|Lamington Volcanics|61310|6|Mentioned|p22|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|65003|5|Briefly described|p7||Tertiary|Of Clarence-Moreton Basin.||||||30-MAR-12
10120|Lamington Volcanics|69594|6|Mentioned|p545|Cenozoic|Cenozoic|Clarence-Moreton Basin.||||||
10120|Lamington Volcanics|69599|5|Briefly described|p595|Miocene|Miocene|Gold Coast hinterland.|||Chinghee Conglomerate.|Overlies Numinbah Valley Formation.||
10120|Lamington Volcanics|72297|6|Mentioned|p732|Cenozoic|Cenozoic|Perlite is mined at the Numinbah deposit, in the McPherson Ranges SE of Beechmont. The deposit is a zone of volcanic glass within the unit.||||||
10120|Lamington Volcanics|73581|5|Briefly described|p6-7|||Extrusive products of the Tweed Volcano. Intercalated with components of the Main Range and Focal Peak volcanoes.|||Beechmont Basalt, Lismore Basalt, Hobwee Basalt, Blue Knob Basalt|Overlies Albert Basalt, Kyogle Basalt|Sequence of distinct basalt and rhyolite flows and tuff horizons.|
10134|Lancewood Shale|30479|6|Mentioned|p22|||See also Fig.3||||||
10134|Lancewood Shale|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
10134|Lancewood Shale|35054|6|Mentioned|Table 23|||||||||
10134|Lancewood Shale|37572|5|Briefly described|p158|||||||||
10134|Lancewood Shale|38446|6|Mentioned|Table 23|||||||||
10134|Lancewood Shale|39445|5|Briefly described|Table 4|||See also p61, p62.||||||09-DEC-08
10134|Lancewood Shale|44211|14|Not recorded|p101|||||||||
10134|Lancewood Shale|44274|14|Not recorded|Tb.1,opp.p7,11|||Overlies Currant Bush Limestone, possibly equivalent to upper part of Currant Bush Limestone.||||||
10134|Lancewood Shale|44482|14|Not recorded|p.11||Middle Cambrian|(E53-12). Middle Cambrian.||||||09-DEC-08
10134|Lancewood Shale|44926|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
10134|Lancewood Shale|45052|5|Briefly described|p93|||Middle Cambrian.||||||09-DEC-08
10134|Lancewood Shale|45079|5|Briefly described|p30|||Cambrian age||||||
10134|Lancewood Shale|64068|6|Mentioned|p225|||Of Opik (1960). In part replaced by Narpa Group.||||||
10134|Lancewood Shale|65337|5|Briefly described|p64.|||Named by Opik (1960). Included in upper Currant Bush Limestone by Smith and Roberts (1963). Reinstated as Lancewood Shale by Shergold et al. (1985). Back as 'provisionally adopted' Currant Bush Limestone in this study.|||||Minor friable sandstone, leached and deeply lateritised siltstone and shale.|
10134|Lancewood Shale|69573|6|Mentioned|p659|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites.||||||
10134|Lancewood Shale|69591|6|Mentioned|p96||||||||Siltstone, shale, chert.|
10146|Landsborough Sandstone|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p494, p496|Aalenian|Rhaetian|Cranfield and Schwarzbock (1976). Nambour Basin. Upper 200m is also known as Brighton beds.|||||A sequence of quartzose sandstones and polymictic conglomerates, followed by sandstone, siltstone, mudstone and coal, then sandstones and coarse pebbly sandstone bands and acritarch-bearing ferruginous oolite.|
10146|Landsborough Sandstone|22845|6|Mentioned|Fig6|Jurassic|Triassic|||||||
10146|Landsborough Sandstone|22846|6|Mentioned|Plate 1|Jurassic|Late Triassic|||||||
10146|Landsborough Sandstone|23251|6|Mentioned|p24|||Overlies sample of North Arm Volcanics dated by K/Ar at 213+/-7Ma, taken from outcrop near the Glass House Mountains.||||||21-JUN-06
10146|Landsborough Sandstone|24081|6|Mentioned|p450|||Geological Province: Nambour Basin.||||||
10146|Landsborough Sandstone|29591|6|Mentioned|p83|||||||||
10146|Landsborough Sandstone|30302|6|Mentioned|p416|||||||||
10146|Landsborough Sandstone|30508|6|Mentioned|p91|||Palynological examination of cores||||||
10146|Landsborough Sandstone|30797|5|Briefly described|Table 1|||Triassic - Jurassic.||||||
10146|Landsborough Sandstone|30914|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
10146|Landsborough Sandstone|32137|6|Mentioned|p355|||Refers oolite beds||||||
10146|Landsborough Sandstone|33288|4|Described|p153|||See also p154 and 155.||||||21-JUN-06
10146|Landsborough Sandstone|33816|6|Mentioned|p492|||||||||
10146|Landsborough Sandstone|33885|6|Mentioned|p492|||||||||
10146|Landsborough Sandstone|33902|6|Mentioned|p127|||See also P128. Map, Jurassic.||||||
10146|Landsborough Sandstone|34287|6|Mentioned|p158|||Triassic||||||
10146|Landsborough Sandstone|35043|6|Mentioned|p78|||||||||
10146|Landsborough Sandstone|35053|5|Briefly described|p36|||||||||
10146|Landsborough Sandstone|35101|6|Mentioned|p49|||||||||
10146|Landsborough Sandstone|35430|6|Mentioned|Fig.2|||Geological map.||||||
10146|Landsborough Sandstone|35866|6|Mentioned|p408|||||||||
10146|Landsborough Sandstone|36238|6|Mentioned|Table 1|||||||||
10146|Landsborough Sandstone|36440|6|Mentioned|Map legend|Early Jurassic|Late Triassic|||||||
10146|Landsborough Sandstone|36547|6|Mentioned|Table 2|||||||||
10146|Landsborough Sandstone|36708|4|Described|p52|||||||||
10146|Landsborough Sandstone|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
10146|Landsborough Sandstone|37456|6|Mentioned|p268|||||||||
10146|Landsborough Sandstone|37463|6|Mentioned|p479|||||||||
10146|Landsborough Sandstone|37616|6|Mentioned|p30|||||||||
10146|Landsborough Sandstone|38074|5|Briefly described|Table 1|||||||||
10146|Landsborough Sandstone|38079|6|Mentioned|p46|||||||||
10146|Landsborough Sandstone|39079|5|Briefly described|p10|||||||||
10146|Landsborough Sandstone|39445|5|Briefly described|Table 10 p132|||||||||29-SEP-05
10146|Landsborough Sandstone|39943|6|Mentioned|Table 12A|||||||||
10146|Landsborough Sandstone|39969|6|Mentioned|p32|||||||||
10146|Landsborough Sandstone|40051|4|Described|p9|||||||||
10146|Landsborough Sandstone|40579|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
10146|Landsborough Sandstone|40623|5|Briefly described|p24|||||||||
10146|Landsborough Sandstone|41917|6|Mentioned|p522|||Shown as Myrtle Creek/Landsborough Sandstone||||||
10146|Landsborough Sandstone|42316|3|Fully described|p7|Early Jurassic|Triassic|Age latest Triassic to late Early Jurassic.||||||
10146|Landsborough Sandstone|42319|5|Briefly described|p3|||||||||
10146|Landsborough Sandstone|42893|2|Defined|p8|Early Jurassic|Late Triassic|||||||
10146|Landsborough Sandstone|42894|5|Briefly described|Fig.1 P20|||||||||
10146|Landsborough Sandstone|42902|5|Briefly described|p418|||||||||
10146|Landsborough Sandstone|43008|5|Briefly described|map legend|||||||||
10146|Landsborough Sandstone|43076|5|Briefly described|p9|||||||||
10146|Landsborough Sandstone|43077|5|Briefly described|p8|||||||||
10146|Landsborough Sandstone|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Nambour Basin.||||||12-APR-05
10146|Landsborough Sandstone|43910|14|Not recorded|p20|||||||||
10146|Landsborough Sandstone|43996|14|Not recorded|p89|||Redated as Jurassic, from palynology in bore at Toorbul Point. See also Lexicon.||||||
10146|Landsborough Sandstone|44091|14|Not recorded|p53||Jurassic|||||||
10146|Landsborough Sandstone|44428|14|Not recorded|p277-278|||Underlies acid phase of North Arm Volcanics probably unconformably.||||||
10146|Landsborough Sandstone|44696|14|Not recorded|p93|||||||||
10146|Landsborough Sandstone|44698|14|Not recorded|p111|||See also Lexicon.||||||
10146|Landsborough Sandstone|44752|14|Not recorded|p297|||Equivalent of Bundamba Group in Maryborough Basin||||||
10146|Landsborough Sandstone|44754|14|Not recorded|p10||Triassic|||||||
10146|Landsborough Sandstone|44783|14|Not recorded|p11,21-3,31,33,39-40|||||||||
10146|Landsborough Sandstone|44813|14|Not recorded|p82||Early Jurassic|||||||
10146|Landsborough Sandstone|44814|14|Not recorded|p485,486|||Lower Jurassic at least in part.||||||
10146|Landsborough Sandstone|44925|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
10146|Landsborough Sandstone|60281|5|Briefly described|page vi, p24|Early Jurassic|Late Triassic|Lower part previously known as the Woogaroo Subgroup; upper part formerly called the Marburg Formation. Has good reservoir potential.  Geological Province: Nambour Basin. See also p29.||||||20-JAN-05
10146|Landsborough Sandstone|60997|6|Mentioned|p140|||Includes the Brighton beds? Geological Province: Nambour Basin.||||||
10146|Landsborough Sandstone|60998|5|Briefly described|p144|Early Jurassic|Early Jurassic|Geological Province: Nambour Basin.||||||
10146|Landsborough Sandstone|63187|5|Briefly described|p108|Jurassic|Late Triassic|Intruded by rhyolites and trachytes.||||||
10146|Landsborough Sandstone|63779|6|Mentioned|p1140, p1145|Early Jurassic|Triassic|||||||
10146|Landsborough Sandstone|64289|5|Briefly described|p16|Early Jurassic|Early Juarssic|Geological province: Nambour Basin.||||||07-FEB-11
10146|Landsborough Sandstone|64665|5|Briefly described|p53 Fig.2.|Early Jurassic|Late Triassic|Southern Nambour Basin. Lower part correlates with Ripley Road Sandstone (Clarence-Moreton Basin) and Myrtle Creek Sandstone (Northern Nambour Basin). The middle part correlates with Gatton Sandstone (Clarence-Moreton Basin). The upper 200 m are also referred to as the Brighton beds.||Unit in Woogaroo and Marburg Subgroups.||Overlies Nambour Formation.|Basal high-energy fluvial quartzose sandstones and polymict conglomerates; then mixed fluvial sandstone, silt and mudstone, with thin coals.|
10146|Landsborough Sandstone|67402|5|Briefly described|p254, p255|Hettangian|Norian|Nambour Basin. Deposited in a fluvial environment. More than 300m thick.|||||Fine-very coarse grained, immature lithic massive sandstones interbedded with thin carbonaceous coaly siltstones and conglomerates.|
10146|Landsborough Sandstone|68008|5|Briefly described|p238|Early Jurassic|Early Jurassic|Nambour Basin. Coeval with Evergreen Formation on the basis of a distinctive oolitic ironstone marker bed.||||||
10146|Landsborough Sandstone|68135|5|Briefly described|p52 fig 2b|Pleinsbachian|Hettangian|Southern Nambour Basin. Contains plant macrofossils and vertebrate body parts.||||Overlain by Brighton beds.|Cross-bedded sandstone.|14-SEP-17
10146|Landsborough Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Bundamba Group, and the Marburg and Woogaroo Subgroups, are all mapped under the symbol, RJb.||||||
10146|Landsborough Sandstone|68576|6|Mentioned|Q_8B: p13|Jurassic|Triassic|Caloundra headland. Sequence of fluviatile sediments.||||||
10146|Landsborough Sandstone|69594|5|Briefly described|p519, p545-547, p572|Early Jurassic|Early Jurassic-Plien (6)|Southern Nambour Basin. Cranfield et al. (1986) and others included the Brighton beds in this unit. Equivalent in part to upper Woogaroo and lower Marburg Subgroups of the Clarance-Moreton Basin.||||Overlies Nambour Formation. Is overlain by Brighton beds? Equivalent to Marburg Subgroup in part.|Fine to coarse, massive quartz and sublabile sandstone overlain by fine to medium, less quartzose labile to sublabile sandstone with minor conglomerate, siltstone, shale and coal.|21-NOV-21
10146|Landsborough Sandstone|69599|5|Briefly described|p595, p638|||Nambour Basin. Is intruded by the Cenozoic Glass House Mountains rhyolite and trachyte..||||Is overlain unconformably by Pomona beds.||21-NOV-21
10146|Landsborough Sandstone|72297|5|Briefly described|p748|||Nambour Basin. Has a limited potential as hydrocarbon source rock. The lower part appears suitable as a reservoir.||||Part of/equivalent to Woogaroo Subgroup.|Includes thin coal and carbonaceous shales.|
10174|Lankelly Suite|22780|5|Briefly described|map|Devonian|Late Silurian|||||||
10174|Lankelly Suite|22781|4|Described|p30|Paleozoic|Paleozoic|Kintore Supersuite||||||07-NOV-08
10174|Lankelly Suite|23420|4|Described|p 151 table 4.8||Early Devonian|Also see p 147 table 4.6. In the Kintore Supersuite.||||||
10174|Lankelly Suite|42610|5|Briefly described|p18|||NOT variation on Lankelly Granite. Part of Kintore Supersuite. Igneous equivalent of Group?||||||
10174|Lankelly Suite|42650|6|Mentioned|p14|||||||||
10174|Lankelly Suite|43596|4|Described|p31-32, p28 Tb. 3|Palaeozoic|Palaeozoic|Of the Kintore Supersuite. Contains Turtle Swamp Granite.||||||15-JAN-09
10174|Lankelly Suite|43738|5|Briefly described|p5|Devonian|Silurian|||||||
10174|Lankelly Suite|43741|6|Mentioned|p7,21|Devonian|Silurian|||||||
10174|Lankelly Suite|43820|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kintore Supersuite||||||24-JAN-05
10174|Lankelly Suite|71849|4|Described|p2-3, p8, p13, p15, p50, p91, p94, p102|Devonian|Devonian|See also p104, p111, p148, p150-154, p156, p158-162, p184, p195. Coen Inlier. Generally much more highly porphyritic than Ebagoola Suite units. Geochemistry detailed.||Kintore Supersuite.|Emu Yard Granite, Lankelly Granite, Leo Creek Granodiorite.||Characteristically highly and coarsely porphyritic, biotite-rich, and with K-feldspar phenocrysts commonly 3-5cm long. Flow alignment common. S-type.|
10174|Lankelly Suite|71854|5|Briefly described|Map legend.|Early Devonian|Early Devonian|||Kintore Supersuite.|Emu Yard, Kendle River, Lankelly Granites; Leo Creek Granodiorite.|||
10261|Lawn Hill Formation|22453|6|Mentioned|p 12|||Geological Province: McArthur Basin.||||||13-OCT-06
10261|Lawn Hill Formation|22665|5|Briefly described|Table1 P222, P227||Calymmian|Actually spelt Lawn Hill Fmn.||||||13-OCT-06
10261|Lawn Hill Formation|22680|6|Mentioned|83,87|||Geol province Mount Isa Basin. Parent McNamara Group||||||
10261|Lawn Hill Formation|22747|5|Briefly described|p8||Precambrian|Conformably overlies Ploughed Mountain Beds||||||
10261|Lawn Hill Formation|23031|6|Mentioned|40|||Geol province Lawn Hill Subprovince. Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23072|5|Briefly described|p753-754||Proterozoic|||||||
10261|Lawn Hill Formation|23075|5|Briefly described|p730|||Of the McNamara Group.||||||
10261|Lawn Hill Formation|23362|6|Mentioned|339 Fig.2|||||||||
10261|Lawn Hill Formation|23363|5|Briefly described|351 Tab.1|Calymmian|Statherian|Ages: 1595+/-6Ma, 1593+/-8Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
10261|Lawn Hill Formation|23393|4|Described|p21|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies the Termite Range Formation.  Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
10261|Lawn Hill Formation|23396|4|Described|p421|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23397|5|Briefly described|p473|||||||||
10261|Lawn Hill Formation|23398|4|Described|p452|Calymmian|Statherian|Age: 1591+/-10Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23405|4|Described|p566|Statherian|Statherian|Of McNamara Group. Age: 1593+/-8Ma.||||||13-OCT-06
10261|Lawn Hill Formation|23406|5|Briefly described|p606,p607 Fig. 8,  p616, p617|Statherian|Statherian|Of McNamara Group. Age: 1591+/-10Ma.||||||16-JUN-09
10261|Lawn Hill Formation|23407|5|Briefly described|p632|||||||||
10261|Lawn Hill Formation|23408|5|Briefly described|p513 Fig.2|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23448|4|Described|p479|||Of McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|23466|5|Briefly described|p272 Fig.6|Calymmian|Statherian|||||||
10261|Lawn Hill Formation|23958|3|Fully described|p1135|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 2200m.||||||07-NOV-08
10261|Lawn Hill Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 2200m.||||||
10261|Lawn Hill Formation|24308|5|Briefly described|p987 Fig. 2|Mesoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
10261|Lawn Hill Formation|24309|5|Briefly described|p1013|Proterozoic|Proterozoic|Of the McNamara Group.||||||13-OCT-06
10261|Lawn Hill Formation|24432|4|Described|p560 Tb.1, p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Termite Range Formation. Age: 1595+/-6 Ma. Siliclastic, carbonaceous and sideritic shale and siltstone. Geological Province: Lawn Hill Platform.||||||
10261|Lawn Hill Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: ~1590Ma.||||||
10261|Lawn Hill Formation|26310|4|Described|p4 Table 1|Proterozoic|Proterozoic|Sandstone, greywacke, shale. Maximum Thickness: 5000 feet. Underlies: Constance Sandstone (unconformably).||||||
10261|Lawn Hill Formation|30508|6|Mentioned|p94|||Stratigraphy||||||
10261|Lawn Hill Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10261|Lawn Hill Formation|31420|6|Mentioned|p216|||||||||
10261|Lawn Hill Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|32660|5|Briefly described|Table 5|||||||||
10261|Lawn Hill Formation|32959|6|Mentioned|Fig.21|||||||||
10261|Lawn Hill Formation|33387|4|Described|p350|||||||||
10261|Lawn Hill Formation|33900|5|Briefly described|p15|||||||||
10261|Lawn Hill Formation|35074|6|Mentioned|Fig.2|||||||||
10261|Lawn Hill Formation|35114|6|Mentioned|Fig.5|||||||||
10261|Lawn Hill Formation|36003|6|Mentioned|Fig.8|||||||||
10261|Lawn Hill Formation|37459|1|Redefined|p432|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||23-DEC-08
10261|Lawn Hill Formation|37568|5|Briefly described|p84|||||||||
10261|Lawn Hill Formation|37569|5|Briefly described|p90|||||||||
10261|Lawn Hill Formation|38237|4|Described|p131|||See also Fig.3.||||||
10261|Lawn Hill Formation|38276|6|Mentioned|Fig.1|||||||||
10261|Lawn Hill Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|38348|4|Described|p22|||||||||
10261|Lawn Hill Formation|38528|6|Mentioned|Fig.1|||||||||
10261|Lawn Hill Formation|38584|6|Mentioned|p22|||||||||
10261|Lawn Hill Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Includes the Widdallion Sandstone Member.  Blocky to massive, thick-bedded, micaceous, cross-bedded medium quartz sandstone.  Conformably overlies the Plain Creek Formation; unconformably overlain by Constance Sandstone.||||||10-JAN-05
10261|Lawn Hill Formation|39445|5|Briefly described|Table 2|||||||||
10261|Lawn Hill Formation|39497|4|Described|p14|||See also Fig.4.||||||13-OCT-06
10261|Lawn Hill Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10261|Lawn Hill Formation|39925|4|Described|p331|||||||||
10261|Lawn Hill Formation|42819|6|Mentioned|p312|||||||||
10261|Lawn Hill Formation|43611|6|Mentioned|p39||Mesoproterozoic|||||||
10261|Lawn Hill Formation|43615|6|Mentioned|p13|||||||||
10261|Lawn Hill Formation|43652|6|Mentioned|p388|||||||||
10261|Lawn Hill Formation|44210|14|Not recorded|p11|||||||||
10261|Lawn Hill Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
10261|Lawn Hill Formation|44238|14|Not recorded|p.221, Fig.1||Precambrian|Defn on Tech.File E/54-9.||||||
10261|Lawn Hill Formation|44271|2|Defined|p36,39,44,57,58|||Conformably overlies Ploughed Mountain Beds. Significant Pb-Zn mineralisation.||||||
10261|Lawn Hill Formation|44274|2|Defined|Tb.2,p9|||||||||
10261|Lawn Hill Formation|44275|14|Not recorded|Map Legend|||||||||
10261|Lawn Hill Formation|44280|14|Not recorded|p6|||||||||
10261|Lawn Hill Formation|44281|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
10261|Lawn Hill Formation|44290|14|Not recorded|p438,439|||Precambrian possibly Palaeoproterozoic.||||||
10261|Lawn Hill Formation|44305|14|Not recorded|p.8|||(E53-8).||||||
10261|Lawn Hill Formation|44482|14|Not recorded|p.6|||(E53-12).||||||
10261|Lawn Hill Formation|44521|14|Not recorded|p8|||Upper Paleoproterozoic.||||||
10261|Lawn Hill Formation|44765|14|Not recorded|p14|||||||||
10261|Lawn Hill Formation|44919|14|Not recorded|p596 (Tb.),p600|||Top of Carpentarian||||||
10261|Lawn Hill Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
10261|Lawn Hill Formation|44989|2|Defined|p.110-112|||Tb. III,IV. On many pages. Underlies Ploughed Mountain Beds. May be roughly equivalent to Cliffdale Volcanics. 2000-5000?' (E54-9).||||||
10261|Lawn Hill Formation|45079|6|Mentioned|p9|||Precambrian age. Map legend P9||||||
10261|Lawn Hill Formation|45166|5|Briefly described|p30|||||||||
10261|Lawn Hill Formation|45287|14|Not recorded|p.225-7,229|||Overlain by Constance Sandstone.||||||
10261|Lawn Hill Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
10261|Lawn Hill Formation|46919|6|Mentioned|p218|||||||||
10261|Lawn Hill Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1595-1630 Ma.Conformably overlies Termite Range Formation. Geological Province: Western Fold Belt.||||||17-DEC-07
10261|Lawn Hill Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Sandstone and conglomeratic sandstone; flaggy tuff and tuffaceous siltstone; carbonaceous shale, micaceous siltstone.||||||
10261|Lawn Hill Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Underlain by Termite Range Formation.||||||03-JUN-09
10261|Lawn Hill Formation|61904|5|Briefly described|p132 Fig. 2|Proterozoic|Proterozoic|Youngest member of the McNamara Group. Includes Bulmung Sandstone Member. Laminated siltstone. Geological Province: Western Fold Belt of Mt. Isa Inlier.||||||
10261|Lawn Hill Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Calvert Superbasin, Western Fold Belt, Mount Isa Inlier.||||||
10261|Lawn Hill Formation|62084|4|Described|p936 Fig.5, p945-946, p949|Proterozoic|Proterozoic|Isa Superbasin. Lawn Hill. Hosts Century deposit (Zn-Pb-Ag stratiform). Age: 1595+/-6 Ma, U-Pb SHRIMP (Page and Sweet 1998). Shown as Lawn Hill Fm. Thickness: 1800-2200 m. Six sedimentary units H1-H6, where H4 is 300 m-thick mineralised sequence.|1611+/-4 U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Variably dolomitic organic siltstones and shales. Shale, siltstone, sandstone, tuffaceous rocks, and minor dolomite.|
10261|Lawn Hill Formation|62659|5|Briefly described|Map Legend|Calymmian|Statherian|Of the McNamara Group. Interlaminated and thinly interbedded red, grey and brown siltstone and fine grained sandstone; green to grey shale and siltstone, dolomitic siltstone, dolostone.||||||
10261|Lawn Hill Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of shale.||||||30-SEP-08
10261|Lawn Hill Formation|63110|6|Mentioned|p1141 Fig. 17|Statherian|Calymmian|Age: ~ 1629-1580Ma. Geological Province: Isa Superbasin.||||||11-JUN-08
10261|Lawn Hill Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Calymmian|Statherian|Of Doom Supersequence.Age: ca. 1575Ma. Thickness: 600-1050m. Geological Province: Isa Superbasin. Consists of volcanic detritus arkose, mudstone, sandstone siltstone, and silty shales.||||||07-FEB-11
10261|Lawn Hill Formation|63113|5|Briefly described|p1214 Fig.2, p1219 Fig.8, p1225 Fig.13. |||Part of Lawn, Wide and Doom supersequences.|c.1615-1589 Ma.|Of the McNamara Group||Overlies Termite Range Formation or Riversleigh Siltstone. Is overlain by Allaru Mudstone.||
10261|Lawn Hill Formation|63114|5|Briefly described|p1253 Fig.2, p1254, p1258. |Proterozoic|Proterozoic|Isa Superbasin. Hosts the stratiform Century Zn-Pb-Ag deposit/Watson's lode.|1595 Ma.|Of the Term, Lawn, Wide and Doom supersequences|||Includes a 45m-thick interlayered black shale and siltstone sequence.|06-APR-17
10261|Lawn Hill Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
10261|Lawn Hill Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300|||Isa superbasin. Material properties detailed.||||||
10261|Lawn Hill Formation|63866|5|Briefly described|p57|Statherian|Statherian|Isa Superbasin. Subdivided into two units in the Term Supersequence and transitional between the Term and Lawn Supersequences.|c. 1636-1611 Ma|||||
10261|Lawn Hill Formation|64250|6|Mentioned|p11 fig 3, p20||||1611 +/- 4 Ma - 1595 +/- 6 Ma|Unit in McNamara Group.||||
10261|Lawn Hill Formation|64317|5|Briefly described|p588 Fig. 1, p589, p595|Mesoproterozoic|Mesoproterozoic|Age for upper section of unit: 1593+/-8Ma. Mainly quartzite, carbonaceous shale and silt/mudstone. Also refers to the 'upper Lawn Hill Formation' which hosts the Century mine.||||||23-SEP-08
10261|Lawn Hill Formation|64575|5|Briefly described|p655, p656 Fig. 1, p657, p664, p665|Proterozoic|Proterozoic|Thickness: >850m. Thick sequence of siltstone, shale and sandstone. Host Century mineralisation.||||||
10261|Lawn Hill Formation|65228|5|Briefly described|p35, Fig.04.|||Lower part of this unit is in the Term Supersequence in the southern Lawn Hill Platform. The upper part is in the Wide Supersequence.||||Overlies Termite Range Formation.||
10261|Lawn Hill Formation|65337|3|Fully described|p9 Fig.5, p29, p33.|Paleoproterozoic|Paleoproterozoic|Formerly Bluff Range beds (Smith and Roberts 1963). 125 - 2600 m of storm-dominated shelf deposits. In Queensland, hosts the world-class Century Zn-Pb-Ag deposit.|c.1616 - c.1595 Ma.|Unit in McNamara Group.|Includes Bulmung and Widdallion Sandstone Members.|Overlies Plain Creek Formation. Is overlain by Playford Sandstone.|Interlaminated and thinly interbedded red, grey and brown siltstone and fine-grained sandstone; green to grey shale and siltstone, dolomitic siltstone, laminated and intraclastic dolostone; distinctive sandstone unit at top.|13-APR-17
10261|Lawn Hill Formation|65396|5|Briefly described|p82, p175, p188, p241|Calymmian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1611 +/- 4 Ma, 1595 +/- 6 Ma|McNamara Group||Overlies Termite Range Formation.||04-APR-17
10261|Lawn Hill Formation|66843|5|Briefly described|p36, p38 Fig.10, p39|||||McNamara Group.|||Includes a basal feldspathic sandstone.|
10261|Lawn Hill Formation|67323|4|Described|Solid Geology Map, p10|Calymmian|Statherian|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Youngest unit in Isa Superbasin sequence. Hosts Zn-Pb Century Mine.|1616 +/- 5 Ma and 1595 +/- 6 Ma.|McNamara Group.|Bulmung Sandstone Member, Widdallion Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite.|
10261|Lawn Hill Formation|68542|5|Briefly described|p4, p6 |||Lawn Hill Platform.|1595 Ma|Upper McNamara Group|||Carbonaceous shale, siltstone and sandstone.|
10261|Lawn Hill Formation|68576|4|Described|Q_2: p4, p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Century Zn deposit (described in detail), and the Zinc Hills Lodes Zn-Pb-Ag deposit.|1595 Ma.|Upper McNamara Group.||Overlies Termite Range Formation. Is overlain unconformably by South Nicholson Group.|A sequence of shale, siltstone and sandstone.|
10261|Lawn Hill Formation|68732|6|Mentioned|p165 Fig.3|||Lawn Hill Platform, Western Fold Belt. Of the Doom Supersequence, Wide Supersequence, Lawn Supersequence, and Term Supersequence. Sedimentary depositional ages.|1595 +/- 6, 1611 +/- 4, 1616 +/- 5 Ma|||||
10261|Lawn Hill Formation|69430|5|Briefly described|p15:39|Proterozoic|Proterozoic|Turbiditic siliciclastic black shale and siderite-rich siltstone host the stratiform Zn-Pb-Ag Century deposit.|||||A succession of shale, siltstone and sandstone.|12-JUL-16
10261|Lawn Hill Formation|69433|4|Described|p18:2, 6, 10|Statherian|Statherian|Sweet (1984); previously mapped as Bluff Range beds (Smith and Roberts, 1963). Southern succession, Lawn Hill Platform. 175-2970m thick, thinning to the N. Marine shelf, mainly below wave-base, deposits. Hosts the world-class Century Zn-Pb-Ag deposit in Qld.; the unit's extension into NT should be considered prospective.||Topmost McNamara Group.|Widdallion Sandstone Member.|Conformably overlies Plain Creek Formation. Is overlain by South Nicholson Group disconformably or locally unconformably.|Recessive, interlaminated and thinly interbedded, grey, green, and red, variably leached, shale, siltstone, very fine-grained sandstone, dolostone and dolomitic siltstone.|12-JUL-16
10261|Lawn Hill Formation|69443|5|Briefly described|p28:19|||Lawn Hill Platform.||McNamara Group.||Is overlain unconformably by Border Waterhole Formation.||12-JUL-16
10261|Lawn Hill Formation|69591|4|Described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Constitutes the Lawn, Wide and Doom Supersequences, separated by disconformities. Deep-marine and proximal submarine fan deposits. Grades downwards into coarser-grained turbidites of Termite Range Formation.|Lower: 1611 +/- 4 Ma (Page et al., 2000).|McNamara Group.||Overlies Termite Range Formation.|Dominantly fine-grained: siltstone, shale, tuff, minor sandstone and dolomite.|
10261|Lawn Hill Formation|69673|4|Described|p52 fig 42, p54, p55|||Up to 2600m thick. Deposited in a marine shelf environment, mainly below wave base. High enough TOC in QLD to be considered valid source rock. Unconventional petroleum potential.||McNamara Group|||Shale, siltstone, very fine grained sandstone, dolostone and dolomitic siltstone.|
10261|Lawn Hill Formation|70897|5|Briefly described|p39-40, Fig.1.7.7|Mesoproterozoic|Mesoproterozoic|Carrara Range region. Age for the H4s siltstone member. Source of abundant reworked sediment, as well as 1591 +/- 10 Ma detrital zircons, in overlying Constance Sandstone.|1595 +/- 6 Ma (Page and Sweet, 1998).|||Is overlain by Constance Sandstone with an angular unconformity (locally disconformably).||
10261|Lawn Hill Formation|71369|5|Briefly described|p4, p8, p13|Calymmian||Age derived from Page et al (2000) who interprets it as the depositional age of tuffs in this unit.|1591 +/- 10 Ma (U-Pb zircon)||Widdallion Sandstone Member.|Is overlain unconformably by Hedleys Sandstone. Is locally overlain by Burangoo Sandstone.||20-FEB-18
10261|Lawn Hill Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1595+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Siltstone, tuffaceous siltstone.|
10261|Lawn Hill Formation|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
10261|Lawn Hill Formation|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|Includes Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuf, minor sandstone, dolomite.|
10261|Lawn Hill Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|
10261|Lawn Hill Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Lithology of numerous other outcrops provided.||Unit of McNamara Group.|Incldues Widdallion Sandstone Member, Bulmung Sandstone Member.||Siltstone, shale, tuff, minor sandstone and dolomite|18-MAR-20
10261|Lawn Hill Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Three ages given as U-Pb zircon sedimentary depositional ages determined from lower and upper parts of the unit in Qld. Base of formation shown as older in NT than Qld.|1615 +/- Ma to 1595 +/- 6 Ma|McNamara Group||Overlies Plain Creek Formation, Termite Range Formation.||
10261|Lawn Hill Formation|72527|5|Briefly described|p7 Fig.1.4, p10, p27, p119, p132.|Paleoproterozoic|Paleoproterozoic|A tuff from the uppermost part of this unit yielded an interpreted magmatic age of 1595 ± 6 Ma. i.e. a minimum age for Lawn Hill Formation. See also p140, p194.|min age from tuff: 1595+/-6 Ma.|McNamara Group||Overlies Plain Creek Formation and underlies Widdallion Sandstone Member. Underlies South Nicholson Group.|Includes tuffs.|
10261|Lawn Hill Formation|72912|4|Described|p5 Fig.3, p14, p32, p33 Fig.12.|Statherian|Statherian|Shown as being located in both Queensland and Northern Territory. Base of unit shown as older in NT. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin.  Three U-Pb zircon sedimentary depositional ages [?] given, also including 1615+/-5 Ma (lower). See also p45-46.|1595+/-6 Ma (upper), 1611+/-4 Ma (lower)|McNamara Group||Overlies Plain Creek Formation (NT) and overlies Termite Range Formation (Qld). Partially equivalent to Doomadgee Formation and Mount Les Siltstone.|Includes organic rich siltstone.|
10261|Lawn Hill Formation|72913|5|Briefly described|p4,7,8, 9 Tb.1, p18, 19 Fig.11, p20,26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in 6 wells in this study. Associated with a gas discovery (Egilabria 2). Mineral composition shows majority quartz, microcline, muscovite, calcite and dolomite.|1611 +/- 4 Ma|McNamara Group||Overlies Termite Range Formation.|Include organic rich siltstone.|
10261|Lawn Hill Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Plain Creek Formation. Probably includes Widdallion Sandstone Member.||
10261|Lawn Hill Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
10261|Lawn Hill Formation|73042|6|Mentioned|p4, p13-14||Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age) (see Fig.1.2).|ca 1615-1595 Ma|McNamara Group||Underlain by Plain Creek Formation and Termite Range Formation. Overlain by(?) Widdallion Sandstone Member and unconformably by South Nicholson Group.||
10261|Lawn Hill Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
10261|Lawn Hill Formation|73098|6|Mentioned|p4, p7, p33|||Lawn Hill Platform. Organic petrolography performed on three samples from the Amoco DDH 83-2 well. [See report for bitumen/maceral description].|||||Includes dark grey shale.|
10261|Lawn Hill Formation|73144|6|Mentioned|p8-9|Calymmian|Statherian|Isa Superbasin. Split across the Doom, Wide, Lawn and Term supersequences. Includes aquifers, partial aquifers, leaky aquitards and aquitards. Includes potential shale gas/oil plays and potential tight gas/oil. Includes oil show and gas discovery in subunit denoted as lower Pmh 4.||McNamara Group|Widdallion Sandstone Member, Bulmung Sandstone Member|Underlain by Termite Range Formation.||14-OCT-22
10294|Lees Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
10294|Lees Sandstone|33164|6|Mentioned|p87|||Correlation. Refers Skwarko (1966).||||||13-OCT-06
10294|Lees Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10294|Lees Sandstone|39445|5|Briefly described|Table 10|||||||||
10294|Lees Sandstone|39523|6|Mentioned|p96|||||||||
10294|Lees Sandstone|44213|14|Not recorded|Map Legend||Late Jurassic|||||||
10294|Lees Sandstone|44989|14|Not recorded|Not recorded|||||||||
10294|Lees Sandstone|45011|4|Described|p9,19,20,22,30|Aptian|Neocomian|On QLD and NT cards. Underlies Polland Shale. Outcrops from Qld border to Pine Creek and beyond.||||||
10294|Lees Sandstone|67323|6|Mentioned|GIS attrib tbl; p106|||informally grouped with Mullaman beds.||||||
10294|Lees Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Tithonian|Carpentaria Basin. Contains plant macrofossils.||||Overlies Hampstead Sandstone|Cross-bedded sandstone.|14-SEP-17
10294|Lees Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Mullaman beds, and unnamed sedimentary units, under the symbol, JKm.||||||
10294|Lees Sandstone|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology maps of the Quamby Project area; mapped as one unit with Mullaman beds and unnamed sediments.||||||
10294|Lees Sandstone|69594|6|Mentioned|p522|||Occurs on the CAMOOWEAL and MOUNT ISA 250k sheets. Known from the NT. Overlies Precambrian and Cambrian basement. Non-marine.||||||
10294|Lees Sandstone|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
10314|Leichhardt Pocket Granite|23426|6|Mentioned|p402.|||||||||
10314|Leichhardt Pocket Granite|23511|5|Briefly described|Map Legend||Early Permian|||||||
10314|Leichhardt Pocket Granite|42369|6|Mentioned|p55|||Intended as an informal name.||||||
10314|Leichhardt Pocket Granite|43070|2|Defined|p30|Early Permian||Of Yates Supersuite.||||||10-SEP-08
10314|Leichhardt Pocket Granite|43098|2|Defined|p34|Early Permian||||||||
10314|Leichhardt Pocket Granite|50596|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Yates Supersuite.  Hornblende-biotite granodiorite and adamellite.||||||
10314|Leichhardt Pocket Granite|60425|5|Briefly described|p54 Tb. 4, p272-3 Appdx. 1|Early Permian|Early Permian|Of Puckley Suite (Yates Supersuite). I-type. Fine-grained, moderately porphyritic hornblende-biotite granite to granodiorite; 'dioritic' enclaves common; accessory minerals present - see p273 for details.||||||07-FEB-11
10314|Leichhardt Pocket Granite|69593|5|Briefly described|p480|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association.||Yates Supersuite.||||
10337|Lena Quartzite Member|23031|6|Mentioned|24|Paleoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Fold Belt. Of the Eastern Creek Volcanics.||||||07-NOV-08
10337|Lena Quartzite Member|23073|6|Mentioned|p745|||||||||
10337|Lena Quartzite Member|23395|5|Briefly described|p386 Fig.3|||Of Eastern Creek Volcanics.||||||13-OCT-06
10337|Lena Quartzite Member|23399|5|Briefly described|p501|||||||||
10337|Lena Quartzite Member|23965|5|Briefly described|p1296|Paleoproterozoic|Paleoproterozoic|Of Eastern Creek Volcanics.  Geological Province: Mount Isa Inlier.||||||07-NOV-08
10337|Lena Quartzite Member|24033|5|Briefly described|p5|||Of Eastern Creek Volcanics. Includes quartzite, feldspathic quartzite and siltstone.||||||
10337|Lena Quartzite Member|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Overlies the Cromwell Metabasalt Member; underlies the Pickwick Metabasalt Member.||||||01-OCT-08
10337|Lena Quartzite Member|30534|2|Defined|p303|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|33900|5|Briefly described|p11|||||||||
10337|Lena Quartzite Member|34499|6|Mentioned|Table 11|||||||||
10337|Lena Quartzite Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|38232|6|Mentioned|p84|||||||||
10337|Lena Quartzite Member|38233|5|Briefly described|Table 1|||||||||
10337|Lena Quartzite Member|38234|6|Mentioned|p103|||||||||
10337|Lena Quartzite Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|38560|6|Mentioned|p113|||||||||
10337|Lena Quartzite Member|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Feldspathic quartzite, orthoquartzite.||||||15-JUN-06
10337|Lena Quartzite Member|39622|6|Mentioned|Appendix|||||||||
10337|Lena Quartzite Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
10337|Lena Quartzite Member|39934|6|Mentioned|p317|||||||||
10337|Lena Quartzite Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10337|Lena Quartzite Member|40221|3|Fully described|p7|||||||||
10337|Lena Quartzite Member|40598|6|Mentioned|Fig.2|||||||||
10337|Lena Quartzite Member|40623|5|Briefly described|p98|||||||||
10337|Lena Quartzite Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
10337|Lena Quartzite Member|42782|6|Mentioned|p469|||Same as Lena Quartzite, Lena Member.||||||13-OCT-06
10337|Lena Quartzite Member|45161|6|Mentioned|p11|||||||||
10337|Lena Quartzite Member|45166|5|Briefly described|p15|||||||||
10337|Lena Quartzite Member|46801|6|Mentioned|p115|||See also Fig. 14.||||||13-OCT-06
10337|Lena Quartzite Member|47083|4|Described|p5-6||Proterozoic|Of Eastern Creek Volcanics (Haslingden Group). Maximum thickness: 200 m.||||||30-JAN-07
10337|Lena Quartzite Member|49009|6|Mentioned|p49|||Member of Eastern Creek Volcanics.||||||
10337|Lena Quartzite Member|50100|5|Briefly described|p17|||Of the Eastern Creek Volcanics.||||||
10337|Lena Quartzite Member|62873|5|Briefly described|p692 Fig. 1|||Also referred to as Lena Quartzite. Separates the Pickwick Metabasalt and Cromwell Metabasalt Members of Eastern Creek Volcanics (above and below respectively).||||||28-NOV-06
10337|Lena Quartzite Member|63023|5|Briefly described|p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Eastern Creek Volcanics (Haslingden Group). Geological Province: Leichardt Superbasin. See also Lena Quartzite (abbrev.).||||||07-NOV-08
10337|Lena Quartzite Member|63111|5|Briefly described|p1164 Tb. 1, p1165|Statherian|Statherian|Of Eastern Creek Volcanics. Overlain by Pickwick Metabasalt Member, underlain by Cromwell Metabasalt Member. Age: 1779+/-4Ma. Thickness: 750m. Geol Prov: Leichhardt Superbasin. Poorly-sorted, coarse-grained to well-sorted, fine-grained sandstone.||||||07-FEB-11
10337|Lena Quartzite Member|67323|4|Described|GIS attrib tbl, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Leichhardt River Domain, Mount Isa Inlier. The rank {Member] is absent in the Eastern Australia Time-Space Plot.|1779 +/- 4 Ma ( MDA: Neumann et al. 2006, 2007).|Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member and is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite, orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|68732|5|Briefly described|p161, p165 Fig.3|Statherian|Statherian|Of the Prize Supersequence. Maximum sedimentary depositional age.|1779 +/- 4 Ma|||||
10337|Lena Quartzite Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member. Is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite and orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Cromwell Metabasalt Member. Is overlain by Pickwick Metabasalt Member.|Feldspathic quartzite and orthoquartzite with rare pebbles.|
10337|Lena Quartzite Member|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1773+/-2 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
10337|Lena Quartzite Member|71799|5|Briefly described|p150 fig 2, p152|Statherian|Statherian|Lawn Hill. 750m thick. Maximum depositional age is derived from Neumann et al, 2006.|1779 +/- 4 Ma (Max. dep. Age)|Eastern Creek Volcanics||Overlies the Cromwell Metabasalt Member. Overlain by the Pickwick Metabasalt Member.|Quartzite, sandstone and greywacke.|
10337|Lena Quartzite Member|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Eastern Creek Volcanics|||feldspathic sandstone, fluvial - coastal.|
10372|Leyburn beds|42901|5|Briefly described|Fig.12 P412|||see also Fig.11 P411||||||
10372|Leyburn beds|43745|6|Mentioned|Fig.4,p13|||||||||
10372|Leyburn beds|60937|5|Briefly described|p424 Fig. 2|||||||||
10392|Lighthouse Granite|9539|5|Briefly described|Map legend|Proterozoic|Proterozoic|White to pink biotite and biotite-muscovite leucogranite, commonly foliated; minor pegmatite. Age: Mid-Proterozoic?||||||02-JUL-15
10392|Lighthouse Granite|23291|5|Briefly described|p88 Tb. 3.7|Mesoproterozoic|Mesoproterozoic|Of the Lighthouse Supersuite. Age:1503+/-33 Ma (Black & Holmes, unpub.ms.); 1561+/-10 Ma (OZCHR). Geological Province: Georgetown Region.||||||08-JUL-15
10392|Lighthouse Granite|23430|5|Briefly described|Table 14.2 p460.||Mesoproterozoic|Zircon crystallisation age 1561 +/- 10 Ma. In the Forsayth Subprovince.||||||16-JAN-07
10392|Lighthouse Granite|23513|5|Briefly described|Map legend||Proterozoic|Proterozoic Intrusive No. 813. ?S-Type.||||||
10392|Lighthouse Granite|24485|6|Mentioned|p19 Tb.1|||||||||
10392|Lighthouse Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10392|Lighthouse Granite|33909|2|Defined|p229|Proterozoic|Proterozoic|||||||
10392|Lighthouse Granite|35214|6|Mentioned|p7|||||||||
10392|Lighthouse Granite|37570|4|Described|p119|||See also p113.||||||16-JAN-07
10392|Lighthouse Granite|39445|5|Briefly described|Table 2|||See also p45.||||||16-JAN-07
10392|Lighthouse Granite|39687|6|Mentioned|p3|||||||||
10392|Lighthouse Granite|39917|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
10392|Lighthouse Granite|41272|5|Briefly described|M 1of1 F04|||||||||
10392|Lighthouse Granite|43259|4|Described|Appendix 1,p53.||Proterozoic|Middle Proterozoic.||||||03-DEC-13
10392|Lighthouse Granite|43664|6|Mentioned|p93|||||||||
10392|Lighthouse Granite|43793|5|Briefly described|p332|||U-Pb age: 1561+/-10 Ma.||||||16-JAN-07
10392|Lighthouse Granite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
10392|Lighthouse Granite|50537|5|Briefly described|p5.1|Mesoproterozoic|Mesoproterozoic|Of the Lighthouse Suite. Geological Province: Georgetown Inlier. Age: 1561 +/- 10Ma (Shrimp).||||||
10392|Lighthouse Granite|61258|6|Mentioned|p389|Mesoproterozoic|Mesoproterozoic|Age: 1561+/-10Ma (Black and Withnall 1993).||||||
10392|Lighthouse Granite|66800|6|Mentioned|p926.||||1561 +/- 10 Ma (Black & Withnall 1993).|||||
10392|Lighthouse Granite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||White and grey foliated, medium-grained, muscovite-biotite leucogranite and pegmatite, commonly with conspicuous mesocratic layers and mafic clots and schlieren; commonly forms swarms of dykes with abundant metamorphic screens.|
10392|Lighthouse Granite|68576|6|Mentioned|Q_11: p24|Mesoproterozoic|Mesoproterozoic|Georgetown area.||||||
10392|Lighthouse Granite|69591|5|Briefly described|p81|Mesoproterozoic|Mesoproterozoic|Withnall et al. (1976). Forsayth Batholith. Small (0.01-1.0 km2) plutons.||Lighthouse Suite.|||Grey/white gneissic to pegmatitic garnetiferous biotite-muscovite leucogranite.|
10392|Lighthouse Granite|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1561+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
10392|Lighthouse Granite|73527|6|Mentioned|p2|||Georgetown Inlier, central domain.||Forsayth Supersuite||||
10392|Lighthouse Granite|73642|5|Briefly described|p4 Tb.1, p10 Fig.8|Calymmian|Calymmian|Georgetown Inlier.|1561+/-20 Ma|Forsayth Supersuite (?)||||
10392|Lighthouse Granite|75079|6|Mentioned|p3, 6, 10-12|Mesoproterozoic|Mesoproterozoic|Northeast Queensland. Major/trace element classification diagrams. Zircon, monazite saturation temperature values diagrams.|~1550 Ma.|Forsayth Supersuite.||||
10410|Lilyvale beds|36228|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
10410|Lilyvale beds|42637|6|Mentioned|p42|||||||||
10410|Lilyvale beds|42640|5|Briefly described|p12|||||||||
10410|Lilyvale beds|42650|5|Briefly described|p18|||||||||
10410|Lilyvale beds|61155|5|Briefly described|p20|Late Miocene|Middle Miocene|Thickness together with Yam Creek beds: 65m. In eastern Cape York.||||||
10410|Lilyvale beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as the Falloch, Wyaaba and Yam Creek beds, are all mapped under the symbol, Tu.||||||
10410|Lilyvale beds|69599|5|Briefly described|p580, p585, p606|Pliocene|Miocene|Carpentaria region. Up to 50m thick. Silcrete weathered surface. Appears as Lilydale beds on p606.||||Correlated with Yam Creek, Wyaaba and Falloch beds.||
10410|Lilyvale beds|71792|5|Briefly described|p2, p59-p62|Pliocene|Miocene|Appears as Lilyvale Creek beds on p26 and p59.|||||Fluviatile clayey quartzose sand, gravel, interbedded sandy clay; lateritised.|
10410|Lilyvale beds|71849|6|Mentioned|p8, p57, p79, p195|Quaternary|Tertiary|||||Nonconformably overlies Buthen Buthen and McIlwraith Granites.||
10410|Lilyvale beds|71853|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartzose sand, gravel, interbedded sandy clay; fluviatile deposits, lateritised.|
10410|Lilyvale beds|71854|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartzose sand, gravel, interbedded sandy clay; fluviatile deposits; lateritised.|
10415|Lime Creek Metabasalt Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10415|Lime Creek Metabasalt Member|30531|2|Defined|p20|Precambrian|Precambrian|||||||
10415|Lime Creek Metabasalt Member|39622|6|Mentioned|p19|||See also Fig.2||||||
10415|Lime Creek Metabasalt Member|45166|5|Briefly described|p20|||||||||
10415|Lime Creek Metabasalt Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.|||||Metabasalt, basaltic pillow lava, amphibolite.|
10415|Lime Creek Metabasalt Member|69591|5|Briefly described|p35 Fig.2.16|||Mary Kathleen Domain, Mount Isa Province.||Corella Formation.|||Pillow basalt with scapolite porphyroblasts.|
10415|Lime Creek Metabasalt Member|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Corella Formation.|||Metabasalt (locally pillowed) and amphibolite.|
10415|Lime Creek Metabasalt Member|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Corella Formation.|||Metabasalt (locally pillowed) and amphibolite.|
10415|Lime Creek Metabasalt Member|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Corella Formation.|||Metabasalt, locally pillowed, and amphibolite.|
10415|Lime Creek Metabasalt Member|71799|5|Briefly described|p154|||About 500m thick.||Corella Formation|||Thin layer of metabasalt.|
10415|Lime Creek Metabasalt Member|73553|6|Mentioned|p8, p22, p119-p121, p126,|||Mary Kathleen Domain. See also Lime Creek Metabasalt. See also p135, p146, p174, p187-189, p230, p232.||Corella Formation, middle|||Mafic volcanic unit.|03-FEB-23
10451|Lion Creek Limestone|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Crl].  Oolitic limestone, skeletal limestone, lithic and feldspathic labile sandstone.||||||
10451|Lion Creek Limestone|30915|6|Mentioned|p93|||||||||
10451|Lion Creek Limestone|31586|6|Mentioned|p5|||See also map P4 & P7.||||||
10451|Lion Creek Limestone|31587|4|Described|p57|||Corals. See also P58-76.||||||
10451|Lion Creek Limestone|31657|5|Briefly described|p94|||See also P101. U.Tournaisian to U.Visean||||||
10451|Lion Creek Limestone|31659|5|Briefly described|p52||Visean|Topmost unit of Rockhampton Group. Overlies the Malchi Formation. Thickness: 250ft.||||||09-JUN-09
10451|Lion Creek Limestone|32867|6|Mentioned|p56|||||||||
10451|Lion Creek Limestone|32868|6|Mentioned|p208,Fig.7|||||||||
10451|Lion Creek Limestone|34085|6|Mentioned|Cor.chart|||Visean||||||
10451|Lion Creek Limestone|34155|6|Mentioned|p91|||Lower Carboniferous. See also P93.||||||
10451|Lion Creek Limestone|36528|6|Mentioned|p173|||||||||
10451|Lion Creek Limestone|38406|6|Mentioned|p11|||||||||
10451|Lion Creek Limestone|39445|5|Briefly described|Table 6|||||||||
10451|Lion Creek Limestone|39973|6|Mentioned|p2|||||||||
10451|Lion Creek Limestone|41576|4|Described|Table 1|||||||||
10451|Lion Creek Limestone|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
10451|Lion Creek Limestone|41925|6|Mentioned|p45|||||||||
10451|Lion Creek Limestone|42002|6|Mentioned|p96|||||||||
10451|Lion Creek Limestone|42547|4|Described|p51|||||||||
10451|Lion Creek Limestone|43538|14|Not recorded|p12,18,35||Early Carboniferous|||||||
10451|Lion Creek Limestone|43983|14|Not recorded|p2||Visean|||||||
10451|Lion Creek Limestone|44091|14|Not recorded|p37||Early Carboniferous|||||||
10451|Lion Creek Limestone|44360|14|Not recorded|p4,30,31||Early Carboniferous|See also Lexicon.||||||
10451|Lion Creek Limestone|44369|14|Not recorded|p174|||Upper limit of Rockhampton Group. Visean fauna of corals.||||||
10451|Lion Creek Limestone|44372|6|Mentioned|p41|||||||||
10451|Lion Creek Limestone|44379|14|Not recorded|p15|||Unit of Rockhampton Group.||||||
10451|Lion Creek Limestone|44388|14|Not recorded|p113-116||Visean|See also Lexicon. Conformably overlies Malchi Formation. Overlain by Neerkol Formation.||||||
10451|Lion Creek Limestone|44432|14|Not recorded|p33,34||Visean|Part of Rockhampton Series.||||||
10451|Lion Creek Limestone|44486|14|Not recorded|p219,220|||||||||
10451|Lion Creek Limestone|45031|14|Not recorded|p31||Early Carboniferous|||||||
10451|Lion Creek Limestone|45097|6|Mentioned|p23|||Late Visean. Correlation chart.||||||
10451|Lion Creek Limestone|46803|6|Mentioned|p143|||Refers Jull (1969)||||||
10451|Lion Creek Limestone|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Rockhampton Group.||||||17-MAY-04
10451|Lion Creek Limestone|61557|5|Briefly described|p892.|||The coral-rich facies developed only after the mobile sand sea floor was stabilized and considerable relief had been developed by the thrombolite-lithistid sponge facies. These reefs also contained the important reef-building calcimicrobe Renalcis.|||||The two main reef-framework facies are thrombolite-lithistid sponges, and coral-boundstone core facies containing >75% rugose and tabulate corals.|
10451|Lion Creek Limestone|68008|4|Described|p90-91, p93, p95-96, p105|Early Carboniferous|Early Carboniferous|Fleming (1967). Type section is in the type area at Malchi Creek, W of Mount Lion; upper boundary moved up-section (explained). Not reliably recognised outside the Stanwell area. Detailed facies description.||Rockhampton Group.|||Contains abundant reef limestones over relatively wide areas.|
10451|Lion Creek Limestone|68679|6|Mentioned|p340|||Fleming (1967).||Rockhampton Group.||||
10451|Lion Creek Limestone|70050|5|Briefly described|p327, p335-336, p338, p341-344, p347-350|Visean|Visean|See also p356-358, p365, p367. N of Stanwell. Contains Cionodendron and Australastraea coral fossils (illustrations and systematic palaeontology), including the holotypes of C. fasciculiseptatum and C. prolongatum, and A. arcifera and A. flemingi.||||Correlated biostratigraphically with Kyndalyn Mudstone Member (Merlewood Formation).||
10479|Little Burke Tillite|31645|4|Described|p2|||See also p3-5. U.Proterozoic.||||||30-JAN-07
10479|Little Burke Tillite|32660|5|Briefly described|Table 5|||||||||
10479|Little Burke Tillite|36898|6|Mentioned|p198|||||||||
10479|Little Burke Tillite|37816|6|Mentioned|Map legend|late Adelaidean|late Adelaidean|||||||
10479|Little Burke Tillite|37930|3|Fully described|p528|||||||||
10479|Little Burke Tillite|38157|6|Mentioned|p282|||||||||
10479|Little Burke Tillite|38350|6|Mentioned|p11|||||||||
10479|Little Burke Tillite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
10479|Little Burke Tillite|39445|5|Briefly described|Table 3|||Glacial sediments. See also p56, p62 and Table 3.||||||30-JAN-07
10479|Little Burke Tillite|39690|6|Mentioned|p91|||||||||
10479|Little Burke Tillite|41405|5|Briefly described|p205|||||||||
10479|Little Burke Tillite|45155|6|Mentioned|p28|||Correlation||||||
10479|Little Burke Tillite|45161|6|Mentioned|p67|||||||||
10479|Little Burke Tillite|45166|5|Briefly described|p45|||||||||
10479|Little Burke Tillite|50100|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|Glacial deposits of tillite capped with dolomite. Geological Province: Georgina Basin.||||||03-JUL-13
10479|Little Burke Tillite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Tillite, dolomite.||||||
10479|Little Burke Tillite|64068|4|Described|p46, 54, p viii|Cryogenian||34 m thick. Correlated with Sun Hill, Black Stump, Oorabra Arkoses, Boko, Olympic Formations, Pioneer Sandstone, Mount Doreen Formation.||Of Keepera Group.||Unconformably overlies Overhang Jaspilite; is unconformably overlain by Mount Birnie beds.|Polymict tillite with polished, faceted and striated boulders.|05-APR-12
10479|Little Burke Tillite|65338|6|Mentioned|p60.|||||Unit in Keepera Group.||||
10479|Little Burke Tillite|65489|6|Mentioned|p125|Proterozoic|Proterozoic|Georgina Basin.||||||
10479|Little Burke Tillite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Tillite.|
10479|Little Burke Tillite|68244|6|Mentioned|p659|Neoproterozoic|Neoproterozoic|Georgina Basin, Qld. Small Meoproterozoic outlier glaciogenic deposits. See Little Burke Formation. Previously described by de Keyser (1972).||||||21-JUN-19
10479|Little Burke Tillite|68270|4|Described|p681-683,686-688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section occurs 9 km NE of township of Duchess, on eastern bank of Little Burke River; lat. 21'18.5"S, long. 139'56"E. Exposed in the far southeastern Georgina Basin. Less than 34m thick. Marine till deposit. Cap dolomite related to Elatina glaciation. Correlative to Elatina Formation.||||Overlain unconformably by Mount Birnie beds. Underlain unconformably by basement.|Diamictite and cap dolomite.|03-JUL-19
10479|Little Burke Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
10479|Little Burke Tillite|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump, Gnallan-a-gea and Sun Hill Arkoses and Yardida Tillite, are all mapped under the symbol, -P-Cg.||||||
10479|Little Burke Tillite|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.||Keepera Group.|||Glacial outwash deposits.|12-JUL-16
10479|Little Burke Tillite|69443|5|Briefly described|p28:7-8|Cryogenian|Cryogenian|Georgina Basin.||Keepera Group.||||12-JUL-16
10479|Little Burke Tillite|72684|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||||Shown as older than Shadow Group.|Tillite.|
10487|Little River Coal Measures|23423|4|Described|Table 7.2 p300||Late Permian|Faulted against Yambo Metamorphic Group and Mulgrave and Chillagoe Formation. Evidence for age is plant fossils. Also see p258 + p298.||||||
10487|Little River Coal Measures|23430|4|Described|p517|||Also see page 504 Table 14.5||||||
10487|Little River Coal Measures|23431|5|Briefly described|p539|||||||||
10487|Little River Coal Measures|23511|5|Briefly described|Map Legend||Late Permian|||||||
10487|Little River Coal Measures|24080|5|Briefly described|p445 Fig. 4|Permian|Permian|Sandstone, shale, coal.  Max. thickness: >1000m.  Geological Province: Laura Basin.||||||
10487|Little River Coal Measures|30914|6|Mentioned|Map legend|Permian|Permian|||||||
10487|Little River Coal Measures|32633|5|Briefly described|p437|||||||||
10487|Little River Coal Measures|33772|6|Mentioned|p11|||||||||
10487|Little River Coal Measures|36101|6|Mentioned|p168|||||||||
10487|Little River Coal Measures|37115|6|Mentioned|Fig.1|||||||||
10487|Little River Coal Measures|37137|4|Described|p251|||||||||
10487|Little River Coal Measures|37575|4|Described|p179|||See also P184||||||
10487|Little River Coal Measures|37613|6|Mentioned|p247|||See also Fig.1||||||
10487|Little River Coal Measures|39252|6|Mentioned|Fig. 15|||||||||
10487|Little River Coal Measures|39266|6|Mentioned|p222|||||||||
10487|Little River Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9||||||
10487|Little River Coal Measures|40623|5|Briefly described|p88|||||||||
10487|Little River Coal Measures|40892|6|Mentioned|Fig.2|||||||||
10487|Little River Coal Measures|42187|6|Mentioned|p319|||||||||
10487|Little River Coal Measures|42620|3|Fully described|p171|Late Permian||||||||
10487|Little River Coal Measures|42648|5|Briefly described|p41|||||||||
10487|Little River Coal Measures|43665|6|Mentioned|p21||Permian|||||||
10487|Little River Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
10487|Little River Coal Measures|43896|14|Not recorded|Map Legend||Late Permian|||||||
10487|Little River Coal Measures|43899|14|Not recorded|p274,276||Permian|See also Lexicon.||||||
10487|Little River Coal Measures|44293|14|Not recorded|Map Legend||Permian|||||||
10487|Little River Coal Measures|44294|2|Defined|Tb.2,p12,21,25,map|||Overlies Chillagoe Formation. Underlies Dalrymple Sandstone.||||||
10487|Little River Coal Measures|44575|14|Not recorded|p236|||||||||
10487|Little River Coal Measures|45025|4|Described|p62-3||Late Permian|||||||
10487|Little River Coal Measures|60358|5|Briefly described|Map Legend|Late Permian|Late Permian|Sandstone, siltstone, carbonaceous shale and mudstone; minor coal, cherty mudstone, limestone. Geological Province: Kennedy Province.||||||18-AUG-04
10487|Little River Coal Measures|60425|3|Fully described|p14 Tb. 1, p38, p198|Late Permian|Late Permian|Faulted against Yambo Metamorphic Group in W, and Chillagoe Formation in E. Max. thickness: <1000m. Shallow water, fluvial and/or lacustrine deposits - detailed lithology of the mainly sandstone and siltstone unit is included; coal seams up to ~6m thick.||||||07-FEB-11
10487|Little River Coal Measures|62371|5|Briefly described|p472 Fig.3|Permian|Permian|Deep marine sediments.||||||09-JUN-06
10487|Little River Coal Measures|63140|6|Mentioned|p572 fig 3|Permian|Permian|Hodgkinson Province.||||||
10487|Little River Coal Measures|63154|5|Briefly described|p281 Fig. 3|Permian|Permian|Geological province: Hodgkinson Province.||||||
10487|Little River Coal Measures|66852|6|Mentioned|p940.|Permian|Permian|Subvertical in Hodgkinson Province due to reactivation of the Proterozoic Palmerville Fault in Late Permian and later.||||||
10487|Little River Coal Measures|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek, Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork, Mitchell River and Nychum Volcanics, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
10487|Little River Coal Measures|69030|6|Mentioned|p6|Permian|Permian|Chillagoe Subprovince, Hodgkinson Province.||||||
10487|Little River Coal Measures|69592|5|Briefly described|p230-231, p243, p245|Permian|Permian|Restricted to a fault-bounded tract SW of Laura; a narrow graben up to ~2km wide and 20km long. Abuts the Palmerville Fault; strata are folded with steep dips. Post-Tabberabberan Orogeny. Fluviatile, lacustrine and mire deposits. Has late Permian macroflora.|||||Mainly lithic and feldspathic sandstone and siltstone, interbedded with carbonaceous shale, mudstone and impure coal seams up to ~6m thick, and siliceous, thin-bedded mudstone and impure limestone.|
10487|Little River Coal Measures|72297|5|Briefly described|p697|Permian|Permian|Near the W margin of the Laura Basin. Occupies a downthrown block. Contains seams of poor-quality coal up to 6m thick.||||||
10517|Llanarth Volcanic Member|22800|4|Described|Fig.2 p581, p582|Early Carboniferous|Early Carboniferous|See also Fig.4 p583.||||||10-FEB-09
10517|Llanarth Volcanic Member|32490|4|Described|Table 1|||Upper Devonian -Lower Carboniferous.||||||10-FEB-09
10517|Llanarth Volcanic Member|32493|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian -Lower Carboniferous.||||||10-FEB-09
10517|Llanarth Volcanic Member|34391|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
10517|Llanarth Volcanic Member|45073|6|Mentioned|p24|||Upper unit of St. Anns Formation.||||||10-FEB-09
10517|Llanarth Volcanic Member|60659|5|Briefly described|p12|||Upper volcanic sequence within Saint Anns Formation - fine-grained acid tuffs. Geological Province: Drummond Basin.||||||07-FEB-11
10517|Llanarth Volcanic Member|68731|5|Briefly described|p191 Fig 3.102|Early Carboniferous|Late Devonian|Age constrained by the parent Saint Anns Formation.||Of the Saint Anns Formation.|||Comprises a thick interval of volcaniclastic sandstone.|
10517|Llanarth Volcanic Member|68900|4|Described|p41-p43|||Drummond Basin. Forms resistant ridges and has a distinctive air-photo pattern. Contains common fiamme and lithic fragments which are difficult to distinguish as a result of weathering.||Saint Anns Formation|||Volcaniclastic siltstone, medium- to coarse-grained, pebbly, moderately to poorly sorted cross-bedded sandstones and local crystal-rich, rhyolitic ignimbrite.|02-NOV-22
10517|Llanarth Volcanic Member|73198|4|Described|p500, p502, p509-511, p513-514|||Drummond Basin, north. Part of Cycle 1 of Olgers (1972). Records basin-wide contemporaneous volcanism. Maximum thickness: 1100 m. Volcanic provenance. [See article for petrographic descriptions and data].||Saint Anns Formation||Overlain by Scartwater Formation.|Includes thick-bedded to massive dacitic and rhyolitic crystal-rich and crystal poor ignimbrite and tuff with minor dacitic and rhyolitic lavas, and volcanolithic conglomerates, sandstones and siltstones.|02-NOV-22
10558|Lochness Formation|22438|6|Mentioned|p549, Fig.12|||||||||
10558|Lochness Formation|22457|5|Briefly described|P31|||Of the Haslingden Group.||||||30-OCT-06
10558|Lochness Formation|22585|5|Briefly described|Fig2 P737, Fig3|||Actually spelt Lochness Fm. in text.||||||30-OCT-06
10558|Lochness Formation|23031|5|Briefly described|24|||Geol province: Mount Isa Fold Belt. Of the Myally Subgroup. Overllain by Torpedo Creek Quartzite, Suprise Creek Formation, Quilalar Formation; underlain by Withworth Quartzite.||||||19-DEC-07
10558|Lochness Formation|23395|5|Briefly described|p386 Fig.3|||Of Myally Subgroup.||||||30-OCT-06
10558|Lochness Formation|23396|4|Described|p418|Statherian|Statherian|of Myally Subgroup (Haslingden Group).||||||30-OCT-06
10558|Lochness Formation|23397|6|Mentioned|p464 Fig.3|||||||||
10558|Lochness Formation|23518|4|Described|p11|Proterozoic|Proterozoic|Of Myally Subgroup.  Geological Province: Western Fold Belt.||||||
10558|Lochness Formation|30534|2|Defined|p304|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|33900|4|Described|p12|||||||||
10558|Lochness Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|38232|6|Mentioned|p84|||||||||
10558|Lochness Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|39445|5|Briefly described|Table 2|||See also p40.||||||30-OCT-06
10558|Lochness Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Whitworth Quartzite; underlies the Quilalar Formation.||||||30-OCT-06
10558|Lochness Formation|39622|6|Mentioned|Fig.2|||See also Appendix||||||
10558|Lochness Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
10558|Lochness Formation|40221|3|Fully described|p10|||||||||
10558|Lochness Formation|41277|5|Briefly described|p83|||||||||
10558|Lochness Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
10558|Lochness Formation|41307|4|Described|p11|||||||||
10558|Lochness Formation|42676|5|Briefly described|Fig.2 P41|||||||||
10558|Lochness Formation|42818|4|Described|p211, Table 1 p209|||Of Myally Subgroup.||||||30-OCT-06
10558|Lochness Formation|45166|5|Briefly described|p14|||||||||
10558|Lochness Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
10558|Lochness Formation|46960|6|Mentioned|p222|||||||||
10558|Lochness Formation|47083|4|Described|p7|||Youngest member of Myally Subgp (Haslingden Gp). Contains 3 informal members. Intruded by Weberra Granite. Conformably overlain by Quilalar Fm; conformably underlain by Whitworth Quartzite.||||||30-OCT-06
10558|Lochness Formation|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
10558|Lochness Formation|50550|6|Mentioned|p1144 Fig.7||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
10558|Lochness Formation|62988|5|Briefly described|p34|||Redbed playa facies. Geological Province: Mount Isa Inlier.||||||25-JAN-07
10558|Lochness Formation|63023|5|Briefly described|p1025 Fig. 2|||Of Myally Subgroup (Haslingden Group). Overlies Whitworth Quartzite; unconformably overlain by Quilalar Formation. Geological Province: Leichardt Superbasin.||||||
10558|Lochness Formation|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Quilalar Formation, underlain by Whitworth Quartzite. Geological Province: Leichhardt Superbasin. Consists of siltstone.||||||
10558|Lochness Formation|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Myally Subgroup. Overlain by Quilalar Formation, underlain by Whitworth Quartzite. Geological Province: Leichhardt Superbasin. Consists mostly of sandstone.||||||07-FEB-11
10558|Lochness Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Whitworth Quartzite. Is overlain by Quilalar Formation.||
10558|Lochness Formation|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Whitworth Quartzite. Is overlain by Quilalar Formation.||
10558|Lochness Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
10558|Lochness Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1, |||Leichhardt superbasin. Material properties detailed.||||||
10558|Lochness Formation|64726|6|Mentioned|p87.||||c.1775-1755 Ma.|||||
10558|Lochness Formation|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.||Myally Subgroup|||Sandstone.|
10558|Lochness Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mount Isa Inlier, Leichhardt Superbasin.||Myally Subgroup.|||Dolomitic feldspathic sandstone and siltstone, laminated ferruginous sandstone.|
10558|Lochness Formation|68021|5|Briefly described|p135|Statherian|Statherian|Towards top of Myally Supersequence. May represent excursion into evaporitic or shallow marine conditions.|||||Red beds with minor amounts of intercalated dolostone.|13-DEC-16
10558|Lochness Formation|68732|5|Briefly described|p160-162, p165 Fig.3|||Deposition in ephemeral playa and sandflat/dry mudflat environments. Of the Myally Supersequence.||Haslingden Group.|||Red siltstones and shales with desiccation cracks and weathering profiles, interpreted as paleosols, occur in this Formation.|01-DEC-17
10558|Lochness Formation|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Near shore/fluvial deposits.|||Myally Subgroup.|Overlies Alsace Quartzite.|Dolomitic feldspathic sandstone and siltstone, laminated ferruginous sandstone (redbeds).|
10558|Lochness Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Whitworth Quartzite.|Dolomitic, feldspathic sandstone and siltstone and laminated ferruginous sandstone.|
10558|Lochness Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Whitworth Quartzite.|Dolomitic, feldspathic sandstone and siltstone and laminated ferruginous sandstone.|
10558|Lochness Formation|71799|5|Briefly described|p154|||Leichardt Superbasin.|ca. 1750 Ma||||Stromatolite bearing dolostones.|
10558|Lochness Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Bortala Formation and underlies Whitworth Quartzite.||
10558|Lochness Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Bortala Formation and underlies Whitworth Quartzite.||
10558|Lochness Formation|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
10558|Lochness Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Bortala Formation. Overlain by Whitworth Quartzite.||
10558|Lochness Formation|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
10583|Log Creek Formation|22464|5|Briefly described|p9|Middle Devonian|Middle Devonian|Also p8. Adavale Basin. Overlies Eastwood Beds, overlain by Lissoy Sandstone||||||
10583|Log Creek Formation|22604|5|Briefly described|p442||Devonian|||||||
10583|Log Creek Formation|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|||||||
10583|Log Creek Formation|23834|4|Described|p312|Eifelian|Emsian|Geological Province: Adavale Basin.||||||
10583|Log Creek Formation|29387|6|Mentioned|Table 1|||Refers to Galloway(1970). Devonian.||||||
10583|Log Creek Formation|29390|6|Mentioned|p53|||Location of Gilmore Gas Field trap.||||||
10583|Log Creek Formation|29391|6|Mentioned|Table 2|||See P14.||||||
10583|Log Creek Formation|29393|6|Mentioned|Table 1|||Lower Devonian.||||||
10583|Log Creek Formation|29721|6|Mentioned|Table 38|||||||||
10583|Log Creek Formation|29753|4|Described|Table 2|||||||||
10583|Log Creek Formation|30103|5|Briefly described|p2|||Part of Adavale Group. Table 2 on P5. See also P6.||||||
10583|Log Creek Formation|30104|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
10583|Log Creek Formation|30544|6|Mentioned|Fig.5 P51|||Devonian||||||
10583|Log Creek Formation|30691|4|Described|p20|||Middle Devonian age. See also Table 6||||||
10583|Log Creek Formation|30853|2|Defined|p25|Middle Devonian|Middle Devonian|See also Table 2||||||
10583|Log Creek Formation|30854|4|Described|Table 2|||Middle Devonian age.||||||
10583|Log Creek Formation|30855|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
10583|Log Creek Formation|31431|5|Briefly described|Table 2|||M.Devonian||||||
10583|Log Creek Formation|31436|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
10583|Log Creek Formation|31999|5|Briefly described|p135|||Table 1||||||
10583|Log Creek Formation|32619|6|Mentioned|p462|||Fauna||||||
10583|Log Creek Formation|33069|4|Described|p6|||Mid.Dev.||||||
10583|Log Creek Formation|33074|6|Mentioned|p262|||||||||
10583|Log Creek Formation|33078|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
10583|Log Creek Formation|33087|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
10583|Log Creek Formation|33088|4|Described|Table 2|||Adavale Gp.||||||
10583|Log Creek Formation|33192|6|Mentioned|p19|||||||||
10583|Log Creek Formation|33326|6|Mentioned|p447|||Fauna.||||||
10583|Log Creek Formation|33641|6|Mentioned|p59|||L.-M.Dev.||||||
10583|Log Creek Formation|36643|6|Mentioned|p65|||||||||
10583|Log Creek Formation|37565|6|Mentioned|Fig.6|||||||||
10583|Log Creek Formation|38226|6|Mentioned|p414|||||||||
10583|Log Creek Formation|39445|5|Briefly described|Table 5|||See also P72 & P73. Gilmore gas field||||||
10583|Log Creek Formation|39478|6|Mentioned|Table 1|||||||||
10583|Log Creek Formation|39480|6|Mentioned|p188|||||||||
10583|Log Creek Formation|39482|6|Mentioned|Fig.5|||||||||
10583|Log Creek Formation|39494|6|Mentioned|Fig.3|||||||||
10583|Log Creek Formation|40030|6|Mentioned|Fig.3|||||||||
10583|Log Creek Formation|40322|6|Mentioned|Fig.3|||||||||
10583|Log Creek Formation|40544|6|Mentioned|Fig.4|||||||||
10583|Log Creek Formation|41097|6|Mentioned|Table 1|||||||||
10583|Log Creek Formation|41167|6|Mentioned|p397|||||||||
10583|Log Creek Formation|41198|6|Mentioned|Table 1|||||||||
10583|Log Creek Formation|41208|4|Described|p13|||||||||
10583|Log Creek Formation|41247|6|Mentioned|Fig.5|||||||||
10583|Log Creek Formation|41289|5|Briefly described|p210|||||||||
10583|Log Creek Formation|41492|6|Mentioned|Fig.10|||||||||
10583|Log Creek Formation|42031|5|Briefly described|Fig.8 P766|||||||||
10583|Log Creek Formation|42999|5|Briefly described|p88,Table1,p90|||||||||
10583|Log Creek Formation|43004|5|Briefly described|Table 1,p179|||||||||
10583|Log Creek Formation|43105|5|Briefly described|Fig.5,p10.|||||||||
10583|Log Creek Formation|46881|6|Mentioned|Table 2|||||||||
10583|Log Creek Formation|48920|6|Mentioned|Fig.2|||||||||
10583|Log Creek Formation|62985|5|Briefly described|p16|Eifelian|Eifelian|Unconformably(?) overlies Eastwood Formation. Fluvial deposits, followed by fluvial-deltaic to shallow marine: feldspatho-lithic and quartzose sandstones, siltstone, mudstone, conglomerate and minor limestone. Geol. prov: Adavale Basin.||||||07-FEB-08
10583|Log Creek Formation|64783|1|Redefined|p92-94, 82, 84, 87-91, 95,96,98,100-104|Givetian|Eifelian|Originally, these rocks were part of Etonvale Formation (Phillips Petroleum Company, 1963); called the Gilmore Formation by Slanis and Netzel (1967) and Tanner (1968); renamed for lack of precedence by Galloway (1970) as Log Creek Formation. Revised (Auchincloss, 1976) to encompass "Cooladdi Dolomite Member" and "Bury Limestone Member". Galloway's 1970 type section (2335.4 - 3057.1 m interval in PPC Etonvale-1) included strata which Paten (1977) differentiated as Lissoy Sandstone which he excluded, as well as Cooladdi Dolomite and Bury Limestone. Type section is redefined here to include the interval from 2501m to 3195.5m. Lower boundary redefined on wireline-log interpretation and crinoid data. Upper boundary is redefined to exclude the Lissoy Sandstone of Paten (1977). Age is middle Eifelian to earliest Givetian. Hosts minor hydrocarbons.||||Unconformably overlies Gumbardo Formation. Correlated with Anna Plains Sandstone. Underlies the Lissoy Sandstone conformably and Bury Limestone.|Consists of feldspatholithic and quartzose sandstone, siltstone, mudstone, conglomerate and minor limestone.|15-NOV-17
10583|Log Creek Formation|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Adavale. Appears in text as Log Ck Formation. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
10583|Log Creek Formation|67402|5|Briefly described|p167 fig ADV/WRR3|Givetian|Eifelian|Adavale Basin. Deposited in mixed fluvial/marine grading to purely marine depositional environments. Proven hydrocarbon reservoir with potential to store carbon dioxide. See also p168 tbl ADV/WRR1, p170, fig ADV/WRR8, p172-p174.||||Unconformably overlies the Eastwood beds. Overlain by the Lissoy Sandstone and the Bury Limestone (which it also grades into laterally).|Feldspatholithic and quartz sandstone, siltstone, mudstone, conglomerate and limestone.|
10583|Log Creek Formation|68731|5|Briefly described|p177 Fig 3.91, p179, p181 Tb 3.3, p183|Late Devonian|Middle Devonian|Adavale Basin. Contains spiriferid brachiopods, woody fragments, crinoids, gastropods, and shell fragments. Tentaculites has also been described (Day and McKellar 1962). Deposited during a marine transgression. ~ 36.8-1300 m thick.||||Unconformably underlain by the Gumbardo Formation. Merges laterally with the Bury Limestone.|Comprises feldspatholithic and quartz sandstone, siltstone, mudstone, conglomerate and minor limestone. Sandstone cements and matrices are dolomitic, argillaceous and siliceous.|
10583|Log Creek Formation|72297|6|Mentioned|p746|||Adavale Basin. Hydrocarbon source rocks in the Gilmore gasfield.||||||
10583|Log Creek Formation|73179|6|Mentioned|p1135 Fig.2, p1136, p1137 Fig.4|Givetian|Eifelian|Adavale Basin. Related to marine transgression in the southern and eastern parts of the basin.||||Unconformably underlain by Eastwood Beds.|Includes fine- to very coarse-grained sandstone and pelitic sandstone.|26-SEP-22
10586|Lollypop Formation|23422|5|Briefly described|p180, p205 Table 6.3|Early Carboniferous|Late Devonian|Of Keelbottom Group.||||||
10586|Lollypop Formation|23424|6|Mentioned|p346|||||||||
10586|Lollypop Formation|23430|5|Briefly described|Plate 14.11|||Of Keelbottom Group. Burdekin Basin Province.||||||
10586|Lollypop Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Keelbottom Group.||||||
10586|Lollypop Formation|23522|5|Briefly described|p250 Fig 6|Famennian|Famennian|||||||
10586|Lollypop Formation|23893|5|Briefly described|p16|Early Carboniferous|Late Devonian|Of Keelbottom Group. Geological Province: Burdekin Basin.||||||02-JUL-15
10586|Lollypop Formation|24074|5|Briefly described|p391 Table 2|Famennian|Famennian|Maximum thickness: 450m. Geological Province: Burdekin Basin.||||||02-JUL-15
10586|Lollypop Formation|24577|4|Described|p752 Fig. 1, p755 Fig. 2|Carboniferous|Carboniferous|Of the Keelbottom Group. Overlain by the Hardwick Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
10586|Lollypop Formation|24610|6|Mentioned|p72|||||||||
10586|Lollypop Formation|24613|2|Defined|p9 Fig. 4, p64-65|Famennian|Famennian|Of Keelbottom Gp. Unconformable on Dotswood Group; conformable on Myrtlevale Fm; conformable below Hardwick Fm. Thickness:450m. Geol.prov: Burdekin Basin.Three lithotypes identified: mainly sst, some siltstone, and pebbly beds -detailed lith. included||||||07-FEB-11
10586|Lollypop Formation|24614|4|Described|p191 Fig. 1, p197-8|Famennian|Famennian|Of the Keelbottom Group. Passes gradationally into Hardwick Formation above;overlies Argentine Metamorphics in the Game Hill area. Max. thickness: 820m; 475m at type section. Geological Prov: Burdekin Basin. See also p193 Fig. 2, p196 Fig. 5.||||||27-AUG-14
10586|Lollypop Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
10586|Lollypop Formation|31285|4|Described|p82|||Famennian to Tournaisian||||||
10586|Lollypop Formation|31999|4|Described|p192|||Table 11||||||
10586|Lollypop Formation|32140|4|Described|p7|||U.Dev.-L.Carb.||||||
10586|Lollypop Formation|32169|6|Mentioned|Table 2|||U.Dev.-L.Carb.||||||
10586|Lollypop Formation|32553|4|Described|p48|||||||||
10586|Lollypop Formation|32865|6|Mentioned|p478|||Late Dev. - early Carb.||||||
10586|Lollypop Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Early Carboniferous to Late Devonian||||||
10586|Lollypop Formation|36628|6|Mentioned|p24|||||||||
10586|Lollypop Formation|37573|4|Described|p217|||See also Fig.13 and Fig.14||||||
10586|Lollypop Formation|39445|5|Briefly described|Table 6|||||||||
10586|Lollypop Formation|39686|6|Mentioned|p72|||||||||
10586|Lollypop Formation|39735|6|Mentioned|p18|||||||||
10586|Lollypop Formation|42547|6|Mentioned|p66|||||||||
10586|Lollypop Formation|42689|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
10586|Lollypop Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
10586|Lollypop Formation|42933|5|Briefly described|p164|||||||||
10586|Lollypop Formation|43095|5|Briefly described|Plate 2|||of Keelbottom Group||||||
10586|Lollypop Formation|43461|14|Not recorded|table p618||Tournaisian|||||||
10586|Lollypop Formation|43933|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Of Keelbottom Group.||||||
10586|Lollypop Formation|44058|14|Not recorded|p103,Tb.p104|||||||||
10586|Lollypop Formation|44060|14|Not recorded|Map Legend|Pleistocene|Late Devonian|||||||
10586|Lollypop Formation|44061|4|Described|Table 2|Early Carboniferous|Late Devonian|||||||
10586|Lollypop Formation|44091|14|Not recorded|p46,Tb.3,||Early Carboniferous|||||||
10586|Lollypop Formation|45097|6|Mentioned|p22|||Correlation chart. Conformable on Myrtlevale Fm.||||||
10586|Lollypop Formation|45151|5|Briefly described|Table 6|||||||||
10586|Lollypop Formation|46845|6|Mentioned|Table 1|||||||||
10586|Lollypop Formation|48904|2|Defined|p28|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
10586|Lollypop Formation|65214|6|Mentioned|p280, p283|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
10586|Lollypop Formation|67402|4|Described|p239, p246, p247, p248|Famennian|Famennian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under braided river and alluvial fan conditions.||||Overlies the Myrtlevale Formation. Overlain by the Hardwick Formation.|Sandstones with minor conglomerates and siltstones.|
10586|Lollypop Formation|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Myrtlevale Formation. Is overlain conformably by Hardwick Formation.|Quartzose to feldspathic sandstone and pebbly sandstone, minor quartzose conglomerate and siltstone; plant fossils.|
10586|Lollypop Formation|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin.||Unit in Keelbottom Group.||Conformably overlies Myrtlevale Formation. Is overlain conformably by Hardwick Formation.|Quartzose to feldspathic sandstone and pebbly sandstone, minor quartzose conglomerate and siltstone; plant fossils.|
10586|Lollypop Formation|68419|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.||Of the Keelbottom Group.||Conformably overlain by the Hardwick Formation. Conformably underlain by the Myrtlevale Formation.|Quartzose to feldspathic sandstone and pebbly sandstone, minor quartzose conglomerate and siltstone; plant fossils.|
10586|Lollypop Formation|68420|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin. But map symbol (Dkl) implies unit is entirely Devonian.||Of the Keelbottom Group.||Conformably overlain by the Hardwick Formation. Conformably underlain by the Myrtlevale Formation.|Quartzose to feldspathic sandstone and pebbly sandstone, minor quartzose conglomerate and siltstone; plant fossils.|27-AUG-14
10586|Lollypop Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4, p187|Late Devonian|Late Devonian|Burdekin Basin. < 500 m thick. Characterised by non-marine sandstone, for which paleocurrent observations indicate transport mainly towards the southeast.||Of the Keelbottom Group.|||Comprises medium- to coarse-grained sublabile sandstone, variably pebbly, subordinate pebble to cobble conglomerate, fine sublabile sandstone and micaceous siltstone.|27-AUG-14
10594|Lolworth Igneous Complex|22611|6|Mentioned|Fig2 P186||Early Devonian|||||||
10594|Lolworth Igneous Complex|23032|6|Mentioned|p38|||of the Hughenden 1:250k sheet area to the south. Equivalent to rocks of the Reedy Springs Batholith ?||||||
10594|Lolworth Igneous Complex|23513|5|Briefly described|Map legend|Devonian|Ordovician|Palaeozoic Intrusive No. 78.  I and S_Type.||||||
10594|Lolworth Igneous Complex|29445|6|Mentioned|p91|||Isotopic ages||||||
10594|Lolworth Igneous Complex|29474|6|Mentioned|p9|||||||||
10594|Lolworth Igneous Complex|30151|4|Described|Table 1|||Upper Silurian to Lower Devonian age. See also Fig.3 K/Ar,R6/Sr ages.||||||
10594|Lolworth Igneous Complex|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
10594|Lolworth Igneous Complex|31813|5|Briefly described|p5|||U.Sil. - L.Dev.||||||
10594|Lolworth Igneous Complex|31999|6|Mentioned|p138|||Table 11||||||
10594|Lolworth Igneous Complex|32169|6|Mentioned|Table 2|||Sil.-U.Dev.||||||
10594|Lolworth Igneous Complex|32359|5|Briefly described|p733|||||||||
10594|Lolworth Igneous Complex|32360|6|Mentioned|p742|||||||||
10594|Lolworth Igneous Complex|32553|4|Described|p60|||||||||
10594|Lolworth Igneous Complex|33202|6|Mentioned|p22|||||||||
10594|Lolworth Igneous Complex|33644|6|Mentioned|Map legend|Early Devonian|Late Silurian|U.Sil or L.Dev.||||||
10594|Lolworth Igneous Complex|33648|4|Described|p10|||U.Sil. or L.Dev.||||||
10594|Lolworth Igneous Complex|34409|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian - Lower Devonian||||||
10594|Lolworth Igneous Complex|34573|6|Mentioned|p32|||400my||||||
10594|Lolworth Igneous Complex|35154|6|Mentioned|p307|||||||||
10594|Lolworth Igneous Complex|35304|6|Mentioned|p605|||||||||
10594|Lolworth Igneous Complex|35560|6|Mentioned|p288|||||||||
10594|Lolworth Igneous Complex|36154|6|Mentioned|Fig.3|||||||||
10594|Lolworth Igneous Complex|36472|6|Mentioned|Map legend|Early Devonian|Late Silurian|Early Devonian to Late Silurian||||||
10594|Lolworth Igneous Complex|36561|6|Mentioned|p542|||||||||
10594|Lolworth Igneous Complex|37144|6|Mentioned|p15|||||||||
10594|Lolworth Igneous Complex|37573|6|Mentioned|p201|||||||||
10594|Lolworth Igneous Complex|37764|6|Mentioned|Table 1|||||||||
10594|Lolworth Igneous Complex|39445|5|Briefly described|Table 12|||||||||
10594|Lolworth Igneous Complex|39686|6|Mentioned|Fig.1|||||||||
10594|Lolworth Igneous Complex|39734|6|Mentioned|p21|||||||||
10594|Lolworth Igneous Complex|39735|6|Mentioned|p18|||||||||
10594|Lolworth Igneous Complex|40746|6|Mentioned|p357|||||||||
10594|Lolworth Igneous Complex|40787|5|Briefly described|p336|||||||||
10594|Lolworth Igneous Complex|40958|6|Mentioned|Table 1|||||||||
10594|Lolworth Igneous Complex|40974|6|Mentioned|p205|||||||||
10594|Lolworth Igneous Complex|41260|6|Mentioned|p48|||||||||
10594|Lolworth Igneous Complex|41272|6|Mentioned|M 1of1 A09|||||||||
10594|Lolworth Igneous Complex|41668|6|Mentioned|p6|||||||||
10594|Lolworth Igneous Complex|41675|6|Mentioned|p64|||||||||
10594|Lolworth Igneous Complex|41774|6|Mentioned|p30|||||||||
10594|Lolworth Igneous Complex|42031|5|Briefly described|p764|||||||||
10594|Lolworth Igneous Complex|42279|6|Mentioned|p27|||||||||
10594|Lolworth Igneous Complex|42693|5|Briefly described|map legend|Early Devonian|Silurian|||||||
10594|Lolworth Igneous Complex|43259|4|Described|Appendix 1,p20.|Early Devonian|Late Silurian|Rb-Sr age is 415+/-7 Ma.||||||
10594|Lolworth Igneous Complex|43480|6|Mentioned|4,24|||related to Georgetown granitoids||||||
10594|Lolworth Igneous Complex|43603|5|Briefly described|p8|||||||||
10594|Lolworth Igneous Complex|43999|14|Not recorded|p94|||K/Ar age 400+/-12 Ma.||||||
10594|Lolworth Igneous Complex|44058|14|Not recorded|p100|||400 ma||||||
10594|Lolworth Igneous Complex|44060|14|Not recorded|Map Legend|Early Devonian|Silurian|||||||
10594|Lolworth Igneous Complex|44061|4|Described|Table 1|Early Devonian|Silurian|||||||
10594|Lolworth Igneous Complex|45073|6|Mentioned|p15|||Refers Clarke & Paine (1970)||||||
10594|Lolworth Igneous Complex|45151|6|Mentioned|Table 3|||||||||
10594|Lolworth Igneous Complex|48903|3|Fully described|p20|||See also Table 1. Rb/Sr & K/Ar ages. U.Sil.-L.Dev.||||||
10594|Lolworth Igneous Complex|48904|4|Described|p17|||See Table 1||||||
10594|Lolworth Igneous Complex|48914|3|Fully described|p28|||U.Sil. - L.Dev. New name.||||||
10614|Lone Pine Gravel|39445|5|Briefly described|Table 14|||||||||
10614|Lone Pine Gravel|44703|14|Not recorded|Map||Cenozoic|See also Lexicon.||||||19-NOV-08
10614|Lone Pine Gravel|44708|14|Not recorded|Sheet 2,section||Cenozoic|||||||19-NOV-08
10614|Lone Pine Gravel|44783|14|Not recorded|p2(Tb.1.)|||||||||
10614|Lone Pine Gravel|69599|6|Mentioned|p586|Pliocene|Pliocene|||||Correlated with Witty Gravel.||
10640|Longsight Sandstone|29591|6|Mentioned|Table 72|||||||||
10640|Longsight Sandstone|29961|4|Described|p12|||Cretaceous||||||
10640|Longsight Sandstone|30021|6|Mentioned|p87|||||||||
10640|Longsight Sandstone|30102|4|Described|p26|||See also P17,27,28,29.||||||
10640|Longsight Sandstone|30461|6|Mentioned|p100|||||||||
10640|Longsight Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
10640|Longsight Sandstone|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10640|Longsight Sandstone|32275|6|Mentioned|p8|||Refers Casey (1959)||||||
10640|Longsight Sandstone|32576|6|Mentioned|p51|||||||||
10640|Longsight Sandstone|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|33075|6|Mentioned|p451|||Refers Casey (1959)||||||
10640|Longsight Sandstone|33111|4|Described|p43|||Mention P6.||||||
10640|Longsight Sandstone|33164|6|Mentioned|Fig.4|||||||||
10640|Longsight Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
10640|Longsight Sandstone|33414|6|Mentioned|p212-214,Tb.||Neocomian|||||||
10640|Longsight Sandstone|33638|6|Mentioned|p10|||||||||
10640|Longsight Sandstone|33825|6|Mentioned|p10|||Correlation table||||||
10640|Longsight Sandstone|33964|6|Mentioned|p6|||Refers Casey (1968) & Yeates (1971).||||||
10640|Longsight Sandstone|34454|5|Briefly described|Table 2|||L.Cret.||||||
10640|Longsight Sandstone|34619|6|Mentioned|p.160, Pl.22||Cretaceous|||||||08-APR-13
10640|Longsight Sandstone|34847|6|Mentioned|p37|||||||||
10640|Longsight Sandstone|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10640|Longsight Sandstone|35139|4|Described|Table.2|||||||||
10640|Longsight Sandstone|35811|6|Mentioned|p556|||Exploration carried out.||||||
10640|Longsight Sandstone|39211|6|Mentioned|p26|||||||||
10640|Longsight Sandstone|39445|5|Briefly described|Table 10|||||||||
10640|Longsight Sandstone|41125|6|Mentioned|p42|||||||||
10640|Longsight Sandstone|41247|6|Mentioned|p126|||||||||
10640|Longsight Sandstone|42397|6|Mentioned|Fig.2 P3|||||||||
10640|Longsight Sandstone|42447|6|Mentioned|p5 + Fig. 17|||Part equivalent to Westbourne Formation.||||||
10640|Longsight Sandstone|42474|5|Briefly described|p26|||||||||
10640|Longsight Sandstone|42749|5|Briefly described|p31|||see also Fig.2 P27||||||
10640|Longsight Sandstone|43105|5|Briefly described|Fig.9,p15|||||||||
10640|Longsight Sandstone|43122|5|Briefly described|p23|||see also Fig. 2.||||||
10640|Longsight Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
10640|Longsight Sandstone|43985|4|Described|p8,10-13,Fig.3,Pl.2|||||||||
10640|Longsight Sandstone|44031|14|Not recorded|p5,8|Cretaceous|Jurassic|||||||
10640|Longsight Sandstone|44082|6|Mentioned|Table p34||Aptian|Mention on correlation table of Queensland Cretaceous sediments.||||||
10640|Longsight Sandstone|44087|14|Not recorded|p4,7,opp.7|||||||||
10640|Longsight Sandstone|44119|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44120|14|Not recorded|Map Legend|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44121|14|Not recorded|p5-6,10-12|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|44122|2|Defined|p318-323,Fig.48|||||||||
10640|Longsight Sandstone|44168|4|Described|Tb.1,6,5,10,map|||||||||
10640|Longsight Sandstone|44212|14|Not recorded|p110|||Not on white card.||||||
10640|Longsight Sandstone|44276|4|Described|p25,Tb.2,map|||Aquifer.||||||
10640|Longsight Sandstone|44277|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44291|2|Defined|Tb.1,p6,8,13,14,map||Early Cretaceous|Equivalent to upper part of Blythesdale Group.||||||
10640|Longsight Sandstone|44308|14|Not recorded|p2,11,13,Tb.2||Early Cretaceous|||||||
10640|Longsight Sandstone|44309|2|Defined|Tb.1,p7,13,14,map|||||||||
10640|Longsight Sandstone|44310|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44312|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44326|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44346|14|Not recorded|p4,5,10|||||||||
10640|Longsight Sandstone|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10640|Longsight Sandstone|44362|4|Described|p11,Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|44376|14|Not recorded|p4,5|||||||||
10640|Longsight Sandstone|44406|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44408|14|Not recorded|p4,opp.p6|||||||||
10640|Longsight Sandstone|44469|2|Defined|opp.p.6,p.12, Tb.I||Cretaceous|(F53-12). Rhizocorallium, wood.||||||
10640|Longsight Sandstone|44470|5|Briefly described|map legend||Cretaceous|||||||02-DEC-04
10640|Longsight Sandstone|44543|2|Defined|p34,36||Early Cretaceous|Underlies Wilgunyah Formation.||||||
10640|Longsight Sandstone|44611|14|Not recorded|p22|||||||||
10640|Longsight Sandstone|44634|14|Not recorded|p30|||||||||
10640|Longsight Sandstone|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10640|Longsight Sandstone|45004|14|Not recorded|p.8,20,32,36,38-63|||On many pages.||||||
10640|Longsight Sandstone|45051|6|Mentioned|Fig.2A|||Lower Cretaceous. See also Fig.5A, 3.||||||
10640|Longsight Sandstone|45052|5|Briefly described|p134|||Cretaceous||||||
10640|Longsight Sandstone|45094|6|Mentioned|p9|||Cret.||||||
10640|Longsight Sandstone|45103|6|Mentioned|p5|||||||||
10640|Longsight Sandstone|48906|14|Not recorded|p5,Tb.2,App.C,Pl.1|Early Cretaceous|Late Jurassic|||||||
10640|Longsight Sandstone|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
10640|Longsight Sandstone|49027|5|Briefly described|p21|||||||||
10640|Longsight Sandstone|60122|5|Briefly described|p35|Cretaceous|Cretaceous|Subsumed into Hooray Sandstone, together with the Tarlton Formation (Mond and Harrison, in Senior et al 1978).||||||
10640|Longsight Sandstone|63450|5|Briefly described|p83|Cretaceous|Jurassic|As defined by Casey (1959) contained two distinct facies, a lower fluvial facies and upper glauconitic marine facies. The latter may be equivalent to Cadna-owie Formation.||||||08-APR-13
10640|Longsight Sandstone|66915|5|Briefly described|p9, p11 Fig.7|||Western Eromanga Basin.||||Is overlain by Wallumbilla Formation on western margin of Eromanga Basin, at C-horizon boundary.||
10640|Longsight Sandstone|67323|5|Briefly described|GIS attrib tbl, p92 Fig.12.2|Cretaceous|Jurassic|See also Solid Geology Map. Galilee/Eromanga/Carpentaria Basins.||||Overlies Ethabuka Sandstone. Is overlain by Wallumbilla Formation.|Sandstone, ferruginous sandstone, conglomerate, some siltstone.|
10640|Longsight Sandstone|67402|6|Mentioned|p214|Cretaceous|Cretaceous|Aquifer unit.||||||
10640|Longsight Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
10640|Longsight Sandstone|69457|5|Briefly described|p41:6|||This name was applied (Smith 1963, 1965; Mond and Harrison in Senior et al. 1978) to outliers of Eromanga Basin strata in TOBERMOREY and HAY RIVER map areas. Some were remapped as undifferentiated Jurassic-Cretaceous by Kruse et al. (2002). They are most probably equivalents of the Algebuckina Sandstone (and possibly the Cadna-owie Formation).|||||Mesa-forming planar to cross-bedded, medium-coarse sandstone and minor mudstone, siltstone and conglomerate.|12-JUL-16
10640|Longsight Sandstone|69594|5|Briefly described|p526, p528|Barremian|Callovian|NW Eromanga Basin. Includes outliers of nominally Mesozoic sedimentary rocks that overlie elements of the Georgina Basin and Precambrian Mount Isa Province. Has been correlated with all units ranging from Hutton Sandstone to Wallumbilla Formation.||||Is overlain by Wallumbilla Formation.||
10663|Lorelle Sandstone Member|24069|5|Briefly described|p283 Fig. 3|Permian|Permian|Of Muggleton Formation. Geological Province: Surat Basin.||||||
10663|Lorelle Sandstone Member|24077|5|Briefly described|p411 Tb. 3|Late Permian|Early Permian|Of the Muggleton Formation.  Coarse grained, quartzose sandstone (marine).  Max. thickness: 62m.  Geological Province: Bowen Basin.||||||
10663|Lorelle Sandstone Member|32578|2|Defined|p354|Late Permian|Early Permian|Early ? to Late Perm.||||||
10663|Lorelle Sandstone Member|36739|6|Mentioned|p22|||||||||
10663|Lorelle Sandstone Member|41725|6|Mentioned|p410|||||||||
10663|Lorelle Sandstone Member|45110|6|Mentioned|Table 16|||||||||
10663|Lorelle Sandstone Member|63713|5|Briefly described|p1507 Fig.2, p1528|Roadian|Kungurian|Roma Shelf, Bowen Basin. The rank (Member) is omitted: appears as Lorell SS. Well-log correlation.||Unit in Muggleton Formation.||||
10663|Lorelle Sandstone Member|64856|4|Described|p63-64|Late Permian|Late Permian|Paten and Groves (1974). Quartzose sandstone unit with minor shale, siltstone, coal and tuff, near the middle of the Muggleton Formation. Only locally developed. Age implied to be Late Permian.|| ||||29-NOV-17
10663|Lorelle Sandstone Member|64857|5|Briefly described|p119|Late Permian|Late Permian|Member of the Muggleton Formation.||||||
10663|Lorelle Sandstone Member|68679|5|Briefly described|p382|Permian|Permian|Roma Shelf, Bowen Basin.||Muggleton Formation.|||Coarse quartz sandstone overlying a finer-grained (transgressive phase) succession.|
10666|Loth Formation|9541|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group.  Quartzose clayey sandstone and siltstone.  Overlies Hampstead Sandstone.||||||07-JUL-04
10666|Loth Formation|22744|5|Briefly described|Fig1, P12, Table3||Jurassic|||||||
10666|Loth Formation|23032|5|Briefly described|p47|Late Jurassic||||||||
10666|Loth Formation|23220|6|Mentioned|p16||Mesozoic|||||||
10666|Loth Formation|23291|4|Described|p81 Tb 3.6|Late Jurassic|Late Jurassic|Parent: Eulo Queen Group. Conformably overlies Hampstead Sandstone. Thickness: 50-100m. Geological Province: Georgetown Region.||||||08-JUL-15
10666|Loth Formation|23425|4|Described|p379, Table 9.7 p395.||Late Jurassic|Of Eulo Queen Group. Underlying unit Hamstead Sandstone.  Carpentaria Basin Province.||||||
10666|Loth Formation|23426|5|Briefly described|p402|||Of Eulo Queen Group. Geological Province Carpentaria Basin.||||||
10666|Loth Formation|23846|5|Briefly described|p5|Jurassic|Jurassic|Of the Eulo Queen Group. Geological Province: Eromanga Basin.||||||
10666|Loth Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
10666|Loth Formation|24073|5|Briefly described|p378 Table 2|Mesozoic|Mesozoic|Of Eulo Queen Group.  Maximum thickness: 65m.  Geological Province: Carpentaria Basin.||||||
10666|Loth Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
10666|Loth Formation|30021|6|Mentioned|p95|||||||||
10666|Loth Formation|30587|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
10666|Loth Formation|31121|6|Mentioned|p390|||||||||
10666|Loth Formation|32553|4|Described|p38|||||||||
10666|Loth Formation|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
10666|Loth Formation|33176|6|Mentioned|p171|||||||||
10666|Loth Formation|33182|6|Mentioned|p190|||||||||
10666|Loth Formation|33183|2|Defined|p230|Late Jurassic|Middle Jurassic|Middle to Late Jurassic.||||||08-DEC-08
10666|Loth Formation|33644|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic?Prob.M - U Jurassic M - U||||||
10666|Loth Formation|33648|4|Described|p19|||||||||
10666|Loth Formation|35560|6|Mentioned|p290|||||||||
10666|Loth Formation|35811|5|Briefly described|Table 3|||||||||
10666|Loth Formation|37576|5|Briefly described|p9|||||||||
10666|Loth Formation|37608|3|Fully described|Table 1|||||||||
10666|Loth Formation|38199|6|Mentioned|p421|||||||||
10666|Loth Formation|39445|5|Briefly described|Table 10|||||||||
10666|Loth Formation|39687|6|Mentioned|Fig.5|||||||||
10666|Loth Formation|39917|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
10666|Loth Formation|40218|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Late Jurassic||||||
10666|Loth Formation|41266|6|Mentioned|Fig.3|||||||||
10666|Loth Formation|42061|4|Described|p153|||See also Fig.4||||||
10666|Loth Formation|43286|5|Briefly described|Map Legend||Jurassic|of Eulo Group.||||||
10666|Loth Formation|43603|5|Briefly described|p9|||||||||
10666|Loth Formation|43630|6|Mentioned|Fig.4,p7||Jurassic|||||||
10666|Loth Formation|45145|3|Fully described|Table 5|||||||||
10666|Loth Formation|46791|6|Mentioned|Table 2|||||||||
10666|Loth Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
10666|Loth Formation|49010|6|Mentioned|Fig.4|||Carpentaria Basin||||||
10666|Loth Formation|49011|6|Mentioned|Fig.3|||Carpentaria Basin||||||
10666|Loth Formation|50199|5|Briefly described|Map Legend|Jurassic|Jurassic|Of the Eulo Queen Group.||||||
10666|Loth Formation|50200|5|Briefly described|Map Legend|Jurassic|Jurassic|Of the Eulo Queen Group.||||||
10666|Loth Formation|50210|5|Briefly described|Map Legend|Jurassic|Jurassic|Overlies: Hampstead Sandstone. Underlies: Yappar Formation.  Of the Eulo Queen Group.||||||
10666|Loth Formation|50211|4|Described|Map Legend|Jurassic|Jurassic|Of Eulo Queen Group. Conformably overlain by Gilbert River Formation. Conformably overlies Hampstead Sandstone.||||||14-MAY-04
10666|Loth Formation|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Of the Eulo Queen Group. Overlies: Hampstead Sandstone.  Underlies: Yappar Member.||||||01-JUL-04
10666|Loth Formation|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Eulo Queen Group.  Fine quartz sandstone and siltstone, commonly micaceous and/or feldspathic; pebbly clayey quartz sandstone; minor grey siltstone.  Overlies Hamsptead Sandstone; underlies Yappar Member (Gilbert River Formation).||||||06-JUL-04
10666|Loth Formation|60081|5|Briefly described|Map legend|Late Jurassic|Jurassic|Of the Eulo Queen Group.  Quartzose clayey sandstone and siltstone.||||||
10666|Loth Formation|64707|5|Briefly described|Map legend|Jurassic|Jurassic|Of Eulo Queen Group. Clayey, commonly micaceous, quartzose to feldspathic sandstone, siltstone and mudstone.||||||08-DEC-08
10666|Loth Formation|66529|6|Mentioned|p12 Fig.5 |||Carpentaria Basin.||Unit in Eulo Q Group.||||
10666|Loth Formation|67402|5|Briefly described|p177 tbl CRP/KRM1|Kimmeridgian|Oxfordian|Carpentaria/Karumba Basins.||Eulo Queen Group|||Medium to coarse grained, micaceous clayey quartz sandstone interbedded with subordinate fine-grained sabndstone siltstone and claystone.|
10666|Loth Formation|68349|5|Briefly described|Map legend.|Late Jurassic|Middle Jurassic|Carpentaria Basin.||Unit in Eulo Queen Group.||Conformably overlies Hampstead Sandstone. Is overlain conformably by Yappar Member (Gilbert River Formation).|Clayey, commonly micaceous, quartzose to feldspathic sandstone, siltstone and mudstone.|
10666|Loth Formation|68417|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|Of the Carpentaria Basin.||Of the Eulo Queen Group.||Conformably overlain by the Gilbert River Formation. Conformably underlain by the Hampstead Sandstone.|Clayey, commonly micaceous, quartzose to feldspathic sandstone, siltstone, and mudstone.|
10666|Loth Formation|69594|5|Briefly described|p521-522, p527|Late Jurassic|Late Jurassic|Southern Staaten Sub-basin, Carpentaria Basin. Not differentiated from the Loth Formation in the Eromanga Basin. 50-100m thick. Restricted fluvial deposits. One of the main aquifers in the Basin.||Eulo Queen Group.||Overlies Hampstead Sandstone.|Micaceous clayey quartzose sandstone with subordinate siltstone and claystone.|
10666|Loth Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Carpentaria Basin.||Eulo Queen Group.||Overlies Hampstead Sandstone. Is overlain by Gilbert River FZ.||
10666|Loth Formation|73147|4|Described|p129-136, 138-144|Early Cretaceous|Middle Jurassic|Smart et al. (1971). Gregory Range area. 50 - 100m thick. Fluvial and brackish fluvio-estuarine deposits. Numerous photographs. Facies types described in great detail. An MDA for the top of this Formation is 117 +/- 7.7 Ma, indicating a paraconformity of 30 m.y. within the Formation. Age spectra summary diagrams. Based on this, sediment provenance from the Lachlan Orogen (>1,000 km to the S) is proposed for the lower and middle parts of this unit.|164.5 +/- 2.2 Ma (MDA: U-Pb detrital zircon).|Eulo Queen Group (upper part).||Conformably overlies Hampstead Sandstone. Is overlain conformably by Yappar Member (Gilbert River Formation). Coeval with Walloon Coal Measures.|Lower and upper units of medium-coarse grained, cross-bedded quartzose sandstone with minor siltstone and mudstone, are separated by a distinctive ripple-laminated, micaceous, fine-grained quartzose sandstone and siltstone with minor mudstone.|
10677|Louisa Formation|23496|5|Briefly described|Table 4, p61||Tertiary|~15m thick.||||||
10677|Louisa Formation|23713|6|Mentioned|p39|||||||||
10677|Louisa Formation|24073|6|Mentioned|p378 Table 2|||Geological Province: Carpentaria Basin.||||||
10677|Louisa Formation|31168|4|Described|p14|||See also Table 2.||||||
10677|Louisa Formation|33528|6|Mentioned|Map legend|middle Tertiary|early Tertiary|Early - Middle Tertiary||||||
10677|Louisa Formation|36228|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
10677|Louisa Formation|37607|5|Briefly described|p334|||See also Fig.5||||||
10677|Louisa Formation|39445|5|Briefly described|Table 14|||||||||
10677|Louisa Formation|42637|6|Mentioned|p29|||||||||
10677|Louisa Formation|43254|5|Briefly described|map legend||Tertiary|||||||
10677|Louisa Formation|43285|5|Briefly described|Map Legend||Tertiary|||||||
10677|Louisa Formation|43287|5|Briefly described|Map Legend||Paleogene|||||||07-NOV-08
10677|Louisa Formation|43625|5|Briefly described|p48|||||||||
10677|Louisa Formation|44292|14|Not recorded|Tb.1,opp.p8,11|||||||||
10677|Louisa Formation|44294|14|Not recorded|p15|||Correlated with Tertiary gravel on SD55-13.||||||
10677|Louisa Formation|45025|6|Mentioned|p102|||Ref. to Woods 1961.||||||
10677|Louisa Formation|45145|5|Briefly described|p33|||||||||
10677|Louisa Formation|61155|5|Briefly described|p16|Eocene||Together with Floraville and Bulimba Formations thickness is 140m.  Geological Province: Western Cape York, Karumba Basin.||||||
10677|Louisa Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
10677|Louisa Formation|69599|5|Briefly described|p585, p602|Eocene|Paleocene|Carpentaria region. Capped by laterite and silcrete of the Aurukun Surface.||||Correlated with Fairview Gravel, Floraville and Bulimba Formations.||
10823|Lowmead Formation|39505|6|Mentioned|p170|||||||||
10823|Lowmead Formation|40247|6|Mentioned|p207|||||||||
10823|Lowmead Formation|42975|5|Briefly described|p255|||||||||
10823|Lowmead Formation|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||
10823|Lowmead Formation|68319|5|Briefly described|Map Legend|Eocene|Eocene||||Includes Sonoma Member, Makowata Oil Shale Member, Korenan Oil Shale Member, Wheatley Oil Shale Member, Harpur Creek Member, Hobble Creek Member.|||
10823|Lowmead Formation|68421|5|Briefly described|Map Legend|Eocene|Eocene|Lowmead Graben.|||Includes Korenan Oil Shale Member, Wheatley Oil Shale Member, Harpur Creek Member, and Hobble Creek Member.||Oil shale, claystone and sandstone.|
10823|Lowmead Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
10823|Lowmead Formation|68679|6|Mentioned|p312-313|Paleogene|Paleogene|Northern New England Orogen.||||||
10823|Lowmead Formation|69599|5|Briefly described|p586, p588-589|Eocene|Eocene|McConnochie and Henstridge (1985). Lowmead Graben, 70km S of Gladstone. Stratigraphic column. Lacustrine deposits, with delta sediments towards the top. RELATED UNITS (continued): Also correlated (at least partly) with Flinders Dolomite; Oakdale Sandstone; Elliott, Petrie Formations.|||Hobble Creek, Harpur Creek, Wheatley Oil Shale, Korenan Oil Shale, Makowata Oil Shale, Sonoma, Members.|Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; see COMMENTS for more.||
10823|Lowmead Formation|72297|5|Briefly described|p753, p755|Oligocene|Oligocene|592m thick. Comprises six members, five of which contain oil shale. Hosts the Lowmead oil shale deposit ~70km S of Gladstone (described and estimated resource tabulated).||||||
10844|Lucknow Granite|30102|6|Mentioned|p4|||||||||
10844|Lucknow Granite|43985|14|Not recorded|p12|||||||||
10844|Lucknow Granite|44408|14|Not recorded|p10|||||||||
10844|Lucknow Granite|48906|14|Not recorded|p12,14|||= Williams Granite.||||||
10847|Lucky Springs Formation|40961|6|Mentioned|p239|||||||||
10907|Ma Ma Creek Member|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Koukandowie Formation||||
10907|Ma Ma Creek Member|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Interbedded sandstone, mudstone. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
10907|Ma Ma Creek Member|23799|5|Briefly described|p48 Fig. 3|Toarcian|Pliensbachian|Probably supersedes Ma Ma Creek Sandstone Member. Of the Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||27-AUG-08
10907|Ma Ma Creek Member|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|41591|5|Briefly described|p21|||||||||
10907|Ma Ma Creek Member|41631|4|Described|p19|||See also Fig.2||||||
10907|Ma Ma Creek Member|42248|2|Defined|App.1 P411|Early Jurassic||Definition card approved by NSW. Distribution includes NSW.||||||
10907|Ma Ma Creek Member|42463|6|Mentioned|Fig.3 P170|||||||||
10907|Ma Ma Creek Member|42869|5|Briefly described|p32|||Of Koukandowie Formation.||||||27-AUG-08
10907|Ma Ma Creek Member|42951|5|Briefly described|Fig.11|||of Koukandowie Formation||||||
10907|Ma Ma Creek Member|43736|6|Mentioned|p29|||||||||
10907|Ma Ma Creek Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
10907|Ma Ma Creek Member|60281|5|Briefly described|p30, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation.  Interbedded sandstone, mudstone.  Max. thickness: 50m.  Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60993|5|Briefly described|p6 Fig. 2, p27|||Supersedes Ma Ma Creek Sandstone Member. Of the Koukandowie Formation. Predominantly siltstone and shale; contains an isochronous ferruginous oolite marker bed. Geol. Prov: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60995|4|Described|p67, p51 Fig. 3|Early Jurassic|Early Jurassic|Base of the Koukandowie Formation. Thinly interbedded sandstone, claystone and mudstone. Overlain by Heifer Creek Sandstone Member.  Max. thickness: 50m. Geol. Prov: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60996|5|Briefly described|p72|||Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60997|5|Briefly described|p139 Fig. 1|Toarcian|Toarcian|Of the Koukandowie Formation. Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
10907|Ma Ma Creek Member|60998|5|Briefly described|p146 Fig. 2|||Of the Koukandowie Formation. Consists of upward-coarsening sequences and contains two ferruginous oolite marker beds. Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60999|5|Briefly described|p174|Early Jurassic|Early Jurassic|Basal oolitic unit of Koukandowie Formation. See also Ma-Ma Creek Member.||||||
10907|Ma Ma Creek Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|61006|5|Briefly described|p286|Jurassic|Jurassic|Of the Koukandowie Formation. Potential hydrocarbon seal.||||||
10907|Ma Ma Creek Member|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Early Jurassic|Of the Koukandowie Sandstone. Silty quartz lithic sandstone, claystone, siltstone, chamositic oolite (Qld.). Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. See also p24.||||||
10907|Ma Ma Creek Member|64289|5|Briefly described|p6 Fig. 2|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
10907|Ma Ma Creek Member|64665|5|Briefly described|p53 Fig.2.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with Evergreen Formation (Surat Basin) and Brighton beds (Southern Nambour Basin).||Lower unit in Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|67402|5|Briefly described|p187, p188, p190, p190 fig CLM6, p193|Pliensbachian|Sinemurian|Clarence-Moreton Basin. Represents a change in depositional environment from sandy braided streams to a floodplain environment includingextensive lake and swamp deposits.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 10-50m thick. Deposited as overbank or flood plain facies as part of a mixed fluvial or lacustrine system. Potential hydrocarbon seal unit.||Koukandowie Formation||Overlies the Towallum Basalt. Overlain by the Heifer Creek Sandstone Member.|Interbedded sandstones and mudstones.|
10907|Ma Ma Creek Member|69594|5|Briefly described|p519, p536 Fig.7.17, p544-546, p572|Toarcian|Toarcian|Northern Clarence-Moreton Basin. Has poor outcrop. The ferruginous oolite marker bed is equivalent to the Westgrove Ironstone Member of the Evergreen Formation, and ironstone marker beds in the Brighton beds and Tiaro Coal Measures.||Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member. Age-equivalent of Brighton beds, Tiaro Coal Measures and Westgrove Ironstone Member.|Includes a ferruginous oolite marker bed.|
10907|Ma Ma Creek Member|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Koukandowie Formation.||||
10907|Ma Ma Creek Member|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|71805|5|Briefly described|p76|Toarcian|Pleinsbachian|Clarence-Moreton Basin.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Heifer Creek Sandstone Member.||
10926|MacMillan Formation|22974|6|Mentioned|p17|||||||||
10926|MacMillan Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
10926|MacMillan Formation|22978|6|Mentioned|p148 Fig.1|||||||||
10926|MacMillan Formation|22988|6|Mentioned|p303|||||||||
10926|MacMillan Formation|23000|5|Briefly described|p296|||||||||
10926|MacMillan Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
10926|MacMillan Formation|23444|5|Briefly described|p185|||||||||
10926|MacMillan Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: ~259Ma.  Geological Province: Bowen Basin.||||||
10926|MacMillan Formation|30850|6|Mentioned|p343|||||||||
10926|MacMillan Formation|31687|6|Mentioned|p283|||?lithologic correlative of Exmoor Fm.||||||
10926|MacMillan Formation|31690|6|Mentioned|Fig. 4|||||||||
10926|MacMillan Formation|32689|1|Redefined|p435|Permian|Permian|||||||
10926|MacMillan Formation|33390|4|Described|p5|||||||||
10926|MacMillan Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
10926|MacMillan Formation|35822|6|Mentioned|p40|||||||||
10926|MacMillan Formation|36739|6|Mentioned|p24|||||||||
10926|MacMillan Formation|37612|5|Briefly described|p283|||See also Fig.3||||||
10926|MacMillan Formation|37726|3|Fully described|p149|||||||||
10926|MacMillan Formation|38518|6|Mentioned|Fig.3|||||||||
10926|MacMillan Formation|38958|6|Mentioned|p492|||||||||
10926|MacMillan Formation|39268|6|Mentioned|p269|||||||||
10926|MacMillan Formation|39272|5|Briefly described|p295|||||||||
10926|MacMillan Formation|39273|6|Mentioned|Fig. 2|||||||||
10926|MacMillan Formation|39445|5|Briefly described|Table 8|||||||||
10926|MacMillan Formation|40321|6|Mentioned|p19|||||||||
10926|MacMillan Formation|40539|6|Mentioned|Fig.2|||||||||
10926|MacMillan Formation|41191|6|Mentioned|Fig.3|||||||||
10926|MacMillan Formation|41246|6|Mentioned|Map legend|Permian||||||||
10926|MacMillan Formation|41809|4|Described|p63|||||||||
10926|MacMillan Formation|42091|6|Mentioned|Table 1 P286|||||||||
10926|MacMillan Formation|42250|6|Mentioned|Fig.4 P31|||||||||
10926|MacMillan Formation|42641|6|Mentioned|p112|||||||||
10926|MacMillan Formation|42856|6|Mentioned|Fig.11 P646|||||||||
10926|MacMillan Formation|43580|6|Mentioned|Fig.1,p360|||||||||
10926|MacMillan Formation|67402|6|Mentioned|p85 tbl BWN2|Capitanian|Capitanian|Bowen Basin. Marine transgressive sediments.||||Overlies the German Creek Formation. Overlain by the Rangal Coal Measures.||
10926|MacMillan Formation|70861|5|Briefly described|p37|Late Permian|Late Permian|Of Bowen Basin.||Unit of Blackwater Group.||Overlain by Fair Hill Formation. Underlain by Moranbah Coal Measures, german Creek Fm, Lower Peawaddy Fm.||
10926|MacMillan Formation|70940|5|Briefly described|p844, p850|Permian|Permian|Comet Ridge and northern Taroom Trough, southeast Bowen Basin.||Blackwater Group.||Overlies German Creek Formation. Is overlain by Fair Hill Formation.||
10926|MacMillan Formation|71276|5|Briefly described|p295-297|Lopingian|Lopingian|Bowen Basin. Marine deposits.||||Interfingers with lower part of Peawaddy Formation. Correlates with upper part of Moranbah Coal Measures.||
10926|MacMillan Formation|73305|6|Mentioned|p548 Fig.1, p550 Fig.3, p553, p556 Fig.8|Late Permian|Late Permian|Bowen Basin. Comet Ridge and northern Taroom Trough. Marine phase prior to regressive succession of the Fair Hill Formation.||||Underlies the Fair Hill Formation.||
10926|MacMillan Formation|73625|5|Briefly described|p5 Fig.3, p13, 19|Permian|Permian|Comet Ridge, Bowen Basin.||||Overlies Crocker Sandstone. Is overlain by Fairhill Formation. With the latter, correlates with Peawaddy Formation.|Includes localised, plant-fossil-rich, permineralised peats associated with silica-rich ash deposits.|
10952|Mackunda Formation|12597|5|Briefly described|p492 Tb.1, p500|Cenomanian|Cenomanian|Eromanga Basin. 60m thick.|||||Marginal marine sequence; labile sandstone, siltstone and mudstone, calcareous in part, containing bivalves, ammonites, belemnites, polyzoans and sharks' teeth.|
10952|Mackunda Formation|13497|5|Briefly described|p115 fig 6.33, p146, p149-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the Macunda Formation on p146.||Marree Subgroup||Overlies the Allaru Mudstone and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
10952|Mackunda Formation|22857|5|Briefly described|p296-7 Tb.22.1|Cenomanian|Albian|Of the Rolling Downs Group. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|22865|5|Briefly described|Table22.1p296-7|Cenomanian|Albian|||||||
10952|Mackunda Formation|22883|5|Briefly described|Fig2 P30||Late Cretaceous|Overlying unit is Winton Formation, underlying unit is Allura Mudstone||||||
10952|Mackunda Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
10952|Mackunda Formation|23056|6|Mentioned|12 table 2|||||||||
10952|Mackunda Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||20-FEB-07
10952|Mackunda Formation|23155|4|Described|p33|Early Cretaceous|Early Cretaceous|Determination of the spore-pollen assemblage indicate an Early Cretaceous (Albian) age. The unit conformably overlies both the Allaru Mudstone and Oodnadatta Formation on STRZELECKI.||||||11-NOV-13
10952|Mackunda Formation|23183|6|Mentioned|p223||Albian|||||||
10952|Mackunda Formation|23188|6|Mentioned|p283,287||Albian|||||||
10952|Mackunda Formation|23375|4|Described|Fig2 p265|Cenomanian|Albian|In the Eromanga Basin.||||||31-OCT-06
10952|Mackunda Formation|23425|5|Briefly described|Plate 10.2|||In the Eromanga Basin Province.||||||20-FEB-07
10952|Mackunda Formation|23430|4|Described|p524 Table 14.7|||Eromanga Basin Province. Maximum thickness <275 m.||||||
10952|Mackunda Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Manuka Sub-Group.||||||
10952|Mackunda Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Australian Superbasin.||||||
10952|Mackunda Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
10952|Mackunda Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24175|3|Fully described|p28, p17 Fig. 3|Cenomanian|Albian|Overlain by Winton Formation; overlies Allaru Mudstone. Max. thickness: 57m. Geological Province: Eromanga Basin.||||||11-NOV-13
10952|Mackunda Formation|24204|5|Briefly described|p263 Fig.4, p267|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Underlain by Allaru Formation. Geological Province: Eromanga Basin||||||20-FEB-07
10952|Mackunda Formation|24321|5|Briefly described|Map legend|Cenomanian|Albian|Of the Neales River Group.||||||31-OCT-06
10952|Mackunda Formation|29591|6|Mentioned|p71|||||||||
10952|Mackunda Formation|30019|6|Mentioned|p2|||Upper Albian||||||
10952|Mackunda Formation|30020|6|Mentioned|p35|||||||||
10952|Mackunda Formation|30103|5|Briefly described|p9|||Unit of Rolling Downs Group. Table 3 on p9.||||||31-OCT-06
10952|Mackunda Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|30691|4|Described|p17|||See also p22,Table 4,6. Lower-Upper Cretaceous.||||||31-OCT-06
10952|Mackunda Formation|30804|6|Mentioned|p10|||||||||
10952|Mackunda Formation|30853|5|Briefly described|Table 3|||Albian age||||||
10952|Mackunda Formation|30854|4|Described|Table 4|||Albian||||||
10952|Mackunda Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Rolling Downs Group||||||
10952|Mackunda Formation|30856|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31098|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31145|5|Briefly described|Table 1|||Lower Cretaceous||||||
10952|Mackunda Formation|31208|6|Mentioned|Fig. 7|||||||||
10952|Mackunda Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31431|5|Briefly described|Table 3|||Lower Cretaceous.||||||
10952|Mackunda Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31434|6|Mentioned|p8|||||||||
10952|Mackunda Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10952|Mackunda Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
10952|Mackunda Formation|32314|6|Mentioned|Fig. 4|||||||||
10952|Mackunda Formation|32395|6|Mentioned|p7|||Correlation||||||
10952|Mackunda Formation|32396|6|Mentioned|p9|||Correlated with Normanton Fm.||||||
10952|Mackunda Formation|32553|4|Described|p38|||||||||
10952|Mackunda Formation|32796|6|Mentioned|p303|||||||||
10952|Mackunda Formation|33016|6|Mentioned|p1|||Table on P1||||||
10952|Mackunda Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
10952|Mackunda Formation|33069|4|Described|p7|||L.-U.Cret.||||||
10952|Mackunda Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33075|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
10952|Mackunda Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||20-FEB-07
10952|Mackunda Formation|33089|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
10952|Mackunda Formation|33176|6|Mentioned|p171|||||||||
10952|Mackunda Formation|33182|6|Mentioned|p200|||L.Cret. See also Table 1||||||
10952|Mackunda Formation|33368|6|Mentioned|p25|||Strat.table.||||||
10952|Mackunda Formation|33372|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33414|6|Mentioned|p211|||||||||
10952|Mackunda Formation|33561|6|Mentioned|p102|||||||||
10952|Mackunda Formation|33638|5|Briefly described|Table 1|||||||||
10952|Mackunda Formation|33639|5|Briefly described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33640|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33642|6|Mentioned|p144-5,147-8,Tb.1,|||Refers Vine & Day (1965). Figs. 1 & 2.||||||
10952|Mackunda Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
10952|Mackunda Formation|33825|6|Mentioned|p10|||Correlation table||||||
10952|Mackunda Formation|33832|5|Briefly described|p11|||Stratigraphy and correlation.||||||31-OCT-06
10952|Mackunda Formation|33964|4|Described|p6|||||||||
10952|Mackunda Formation|34065|4|Described|p6|||L.Cret.||||||
10952|Mackunda Formation|34091|5|Briefly described|Table 1|||L.Cret||||||
10952|Mackunda Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34218|4|Described|Table 1|||Lower Cretaceous. See also Table 2.||||||
10952|Mackunda Formation|34356|6|Mentioned|p21|||Albian.||||||
10952|Mackunda Formation|34485|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34486|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34611|6|Mentioned|Fig.65|||Correlation chart||||||
10952|Mackunda Formation|34619|3|Fully described|p.160. Pl.22||Adelaidean|||||||
10952|Mackunda Formation|35139|4|Described|Table.2|||||||||
10952|Mackunda Formation|35239|6|Mentioned|Fig.4|||||||||
10952|Mackunda Formation|35560|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35793|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35811|5|Briefly described|Table 3|||||||||
10952|Mackunda Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
10952|Mackunda Formation|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
10952|Mackunda Formation|36243|6|Mentioned|Table 6A|||||||||
10952|Mackunda Formation|36552|6|Mentioned|Fig.25|||||||||
10952|Mackunda Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
10952|Mackunda Formation|37263|6|Mentioned|p319|||||||||
10952|Mackunda Formation|37451|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|37608|3|Fully described|Table 1|||||||||
10952|Mackunda Formation|38226|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|38373|6|Mentioned|p621|||||||||
10952|Mackunda Formation|38779|6|Mentioned|p4|||||||||
10952|Mackunda Formation|38814|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39070|4|Described|p366|||||||||
10952|Mackunda Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,11,13 etc. Correlation||||||
10952|Mackunda Formation|39445|5|Briefly described|Table 11|||||||||
10952|Mackunda Formation|39478|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39846|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|39847|5|Briefly described|p40|||||||||
10952|Mackunda Formation|39943|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40121|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|40199|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40220|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40249|6|Mentioned|p41|||||||||
10952|Mackunda Formation|40675|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40681|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40687|3|Fully described|p419|||||||||
10952|Mackunda Formation|40801|6|Mentioned|p42|||||||||
10952|Mackunda Formation|40910|6|Mentioned|p17|||||||||
10952|Mackunda Formation|40926|6|Mentioned|p19|||||||||
10952|Mackunda Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
10952|Mackunda Formation|41062|6|Mentioned|Fig.5|||||||||
10952|Mackunda Formation|41063|6|Mentioned|p40|||||||||
10952|Mackunda Formation|41064|6|Mentioned|p62|||||||||
10952|Mackunda Formation|41084|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41085|6|Mentioned|p89|||||||||
10952|Mackunda Formation|41086|3|Fully described|p98, Fig.3|||||||||
10952|Mackunda Formation|41088|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41097|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41099|6|Mentioned|Fig.9|||||||||
10952|Mackunda Formation|41165|5|Briefly described|p363|||Mention Fig.15||||||
10952|Mackunda Formation|41176|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|41177|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41182|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41183|6|Mentioned|Fig.3 p308|||||||||
10952|Mackunda Formation|41187|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41198|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41214|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41216|6|Mentioned|Fig.18|||||||||
10952|Mackunda Formation|41266|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41523|3|Fully described|p282|||See also p277.||||||31-OCT-06
10952|Mackunda Formation|41707|6|Mentioned|Fig.8|||||||||
10952|Mackunda Formation|41724|6|Mentioned|p383|||||||||
10952|Mackunda Formation|41950|5|Briefly described|Fig.2 P3|||||||||
10952|Mackunda Formation|42061|4|Described|Fig,11 P159|||||||||
10952|Mackunda Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||31-OCT-06
10952|Mackunda Formation|42071|6|Mentioned|p117|||||||||
10952|Mackunda Formation|42084|6|Mentioned|Fig.3 P356|||||||||
10952|Mackunda Formation|42085|6|Mentioned|Fig.2 P374|||||||||
10952|Mackunda Formation|42395|5|Briefly described|Fig.13 P83|||||||||
10952|Mackunda Formation|42397|6|Mentioned|Fig.2 P3|||||||||
10952|Mackunda Formation|42429|6|Mentioned|Figs.6 & 9 P156|||||||||
10952|Mackunda Formation|42446|4|Described|p14|||||||||
10952|Mackunda Formation|42447|6|Mentioned|Fig. 1|||||||||
10952|Mackunda Formation|42477|5|Briefly described|p166|||||||||
10952|Mackunda Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
10952|Mackunda Formation|42520|5|Briefly described|p6|||||||||
10952|Mackunda Formation|42673|5|Briefly described|Fig.2, P184|||||||||
10952|Mackunda Formation|42746|5|Briefly described|p12|||See also Fig.6||||||
10952|Mackunda Formation|42749|6|Mentioned|Fig.2 P27|||||||||
10952|Mackunda Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
10952|Mackunda Formation|43002|5|Briefly described|Fig.2,p135|||||||||
10952|Mackunda Formation|43004|5|Briefly described|Table 1,p179|||||||||
10952|Mackunda Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone. Includes Mount Howie Sandstone.||||||25-MAY-05
10952|Mackunda Formation|43105|6|Mentioned|p15|||||||||
10952|Mackunda Formation|43114|5|Briefly described|p16|||||||||
10952|Mackunda Formation|43122|5|Briefly described|Fig.2.|||||||||
10952|Mackunda Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43591|6|Mentioned|p40|||||||||
10952|Mackunda Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44017|14|Not recorded|Map Legend|||||||||
10952|Mackunda Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44020|14|Not recorded|p10,Tb.1,2||Early Cretaceous|Of roling Dwons Grouop.||||||
10952|Mackunda Formation|44031|14|Not recorded|p3,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44033|14|Not recorded|map,p4,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
10952|Mackunda Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44067|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44082|6|Mentioned|p6,12,26,28,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
10952|Mackunda Formation|44089|4|Described|Tb.1,p3,4,8,9,map||Early Cretaceous|||||||
10952|Mackunda Formation|44091|14|Not recorded|p60|||||||||
10952|Mackunda Formation|44133|4|Described|p122-123, 104 Fig. 9.11|Early Cenomanian|Late Albian|Geological Province: Eromanga Basin. Conformably overlies Oodnadatta Formation and Allaru Mudstone. Contains sediments from the now superseded Mount Alexander Sandstone Member and Blanchewater Formation.||||||
10952|Mackunda Formation|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44362|4|Described|p12,Tb.1||Early Cretaceous|||||||
10952|Mackunda Formation|44374|14|Not recorded|p12||Cretaceous|early Late Albian sandstone,siltstone indicating shoaling of seas throughout Eromanga Basin.||||||
10952|Mackunda Formation|44376|14|Not recorded|p6|||||||||
10952|Mackunda Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44414|14|Not recorded|p110-112|||Sandstone, mudstone characterised by marine fossils overlain by Winton Formation.||||||
10952|Mackunda Formation|44417|2|Defined|p416,419-420|||Formerly called Mackunda Beds. Overlies Wilgunya Formation. Albian fossils. Unit of Rolling Downs Group.||||||31-OCT-06
10952|Mackunda Formation|44418|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44573|14|Not recorded|p98||Cretaceous|||||||
10952|Mackunda Formation|44807|14|Not recorded|unknown (p1-16)|||Allaru Mudstone, correlated with Normanton Formation.||||||
10952|Mackunda Formation|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965. Comparable to lower part of Blanchewater Formation in South Australia.||||||
10952|Mackunda Formation|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10952|Mackunda Formation|45052|5|Briefly described|p134|||Mesozoic||||||
10952|Mackunda Formation|45103|6|Mentioned|p8|||||||||
10952|Mackunda Formation|45110|6|Mentioned|p147|||See also Table 18.||||||
10952|Mackunda Formation|45168|6|Mentioned|p6|||||||||
10952|Mackunda Formation|46791|5|Briefly described|p48|||||||||
10952|Mackunda Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
10952|Mackunda Formation|48920|3|Fully described|p62|||||||||
10952|Mackunda Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
10952|Mackunda Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
10952|Mackunda Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Allaru Mudstone. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Allaru Mudstone and Oodnadatta Formation, with which it also interfingers laterally. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
10952|Mackunda Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone.||||||
10952|Mackunda Formation|61312|5|Briefly described|p64, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Siltstone, sandstone, minor shale. Geological Province: Eromanga Basin (absent in NSW).||||||
10952|Mackunda Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
10952|Mackunda Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
10952|Mackunda Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
10952|Mackunda Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
10952|Mackunda Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
10952|Mackunda Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
10952|Mackunda Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta and Allaru Formations. Is overlain by Winton Formation.||
10952|Mackunda Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
10952|Mackunda Formation|63979|2|Defined|p53, Fig. 44|Cenomanian|Albian|Previously Mackunda Beds (Vine 1964). Of Manuka Subgroup (Rolling Downs Gp). Conformable on Allaru Mudstone. Conformable below Winton Fm. Max. thick: 150m. Interbedded sandstone, siltstone and mudstone and lesser mudclast intraformational conglomerate.||||||07-FEB-11
10952|Mackunda Formation|64048|6|Mentioned|p64 Tb. 2, p72|||Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Allaru Mudstone (Marree Subgroup); is overlain by Winton Formation.||10-DEC-15
10952|Mackunda Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
10952|Mackunda Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
10952|Mackunda Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Allaru Mudstone and Oodnadatta Formation. Overlain by Winton Formation.||||||08-MAR-12
10952|Mackunda Formation|65489|5|Briefly described|p49, p55, p58, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 200m thick. Regional seal.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone; siltstone; shale.|
10952|Mackunda Formation|66518|6|Mentioned|p19 Fig.4.|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||06-FEB-14
10952|Mackunda Formation|66529|6|Mentioned|p12 Fig.5, p16  |||||Unit in Rolling Downs Group.||Overlies Oodnadatta Formation and Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|66623|6|Mentioned|pp264-265.|||Partly equivalent to Allaru Mudstone in Koonenberry Belt, NSW.||||Overlies Allaru Mudstone.||
10952|Mackunda Formation|67323|5|Briefly described|p87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.|Feldspathic sandstone, siltstone.|
10952|Mackunda Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Albian|Eromanga Basin. Deposited in shallow marine or paralic environments. Maximum thickness of 100m. Estimated porosity of 10-25% with unknown permeability. See also p108, p109, p115 tbl ERO2.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.|Very fine to fine-grained sandstone, with laminations of siltstone and mudstone and lesser mud-clast intraformational conglomerate.|
10952|Mackunda Formation|67784|5|Briefly described|p25-26, p28-32|Albian|Albian|Northern Eromanga Basin. 90-275m thick.||||Overlies Allaru Formation, overlain by Winton Formation|Contains labeceratid ammonites.|08-FEB-18
10952|Mackunda Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Marginal marine to paralic; a marine regression. Fossiliferous: molluscs, forams, wood, diverse microflora, fish and vertebrates.||Unit in Neales River Group.||Conformably overlies Oodnadatta Formation. Is overlain conformably by Winton Formation.|Bimodal cross-bedded, yellow-brown fine to medium sand interbedded with greenish to grey silt and silty clay; then pale grey-green, interbedded, cross-bedded, glauconitic, sand-silt-shale and calcareous shales, mud and clay intraclasts common.|
10952|Mackunda Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Mackunda Formation as one unit.|||||Mudstone and siltstone.|
10952|Mackunda Formation|68206|6|Mentioned|p31-33|Albian|Albian|NE Eromanga Basin.||||Overlies Allaru Formation.||
10952|Mackunda Formation|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
10952|Mackunda Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.||
10952|Mackunda Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
10952|Mackunda Formation|68715|6|Mentioned|p30 Fig.7|Cenomanian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|68731|6|Mentioned|pp209-211|||||||||
10952|Mackunda Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Marine to coastal paralic. Mis-spelt as Mackundra Formation in Fig.2.||Of the Rolling Downs Group.||||16-JAN-17
10952|Mackunda Formation|68821|5|Briefly described|p292 Fig.1, p296|Cretaceous|Cretaceous|Lower Cretaceous age. Parallic to marine sediments.||Of the Rolling Downs Group.||||
10952|Mackunda Formation|69019|4|Described|p83 Fig.20, p85, p99-101.|Cenomanian|Albian|Of Vine and Day (1965). Eromanga Basin; final Cretaceous marine deposition. Thickness from 0-192 m. Has developed a porcellanite horizon.||Unit in Neales River Group.||Overlies Oodnadatta Formation conformably; overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt; shale and calcareous shale, often as intraclasts in upper sand beds. Contains ovoidal limestone concretions to tabular limestone bodies.|
10952|Mackunda Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93|Cenomanian|Albian|See also p105-106, p119, p122-123, p151, p191-192. Defined by Vine and Day (1965) in Queensland as the youngest marine to marginal marine unit within the Eromanga Basin. Thickness varies from <49 to ~82m. Marginal marine and paralic to deltaic. Diverse fauna listed. Weathering has formed porcellanite. Stratigraphic wells intersection data.||||Conformably overlies Oodnadatta Formation and Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt, shale and calcareous shale. Local ferricrete capping.|
10952|Mackunda Formation|69457|4|Described|p41:2-3, 6-7, 10-12|Early Cretaceous|Early Cretaceous|Vine and Day (1965). Central and southern Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Thickness is variable, from 74m to >150m. Marine; distinguished by its lack of coal. Contains a diverse fossil assemblage, from a dinosaur to microfossils.||Manuka Subgroup.||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Thinly interbedded labile very fine- to fine-grained lithic sandstone, laminated siltstone and mudstone with numerous plant remains, and lesser mud-clast intraformational conglomerate.|12-JUL-16
10952|Mackunda Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|||Said to be a unit in Marree Subgroup.||||06-APR-22
10952|Mackunda Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overrlain by the Winton Formation.||
10952|Mackunda Formation|69594|5|Briefly described|p519, p526, p530-531, p574|Cenomanian|Albian|Vine (1964); Vine and Day (1965). Eromanga Basin. Mostly 75-100+ metres thick. Boundaries in drill holes are distinguished by various geophysical properties (described). Shallow-marine and paralic deposits with abundant volcanilithic sediments from the E. Contains a distinct marine fauna (listed) including the "iconic" Muttaburrasaurus.||||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Labile volcanic lithic-feldspathic interbedded sandstone, siltstone, mudstone and minor impure coquinitic and cone-in-cone limestone and intraformational conglomerate.|
10952|Mackunda Formation|69599|6|Mentioned|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by Moses Sandstone.||
10952|Mackunda Formation|69673|5|Briefly described|p155 fig 127|Cretaceous|Cretaceous|||Manuka Subgroup||Overlies Oodnadatta Formation, Allaru Mudstone, overlain by Winton Formation|Carbonaceous, pyritic shale with lesser interbedded sandstone.|
10952|Mackunda Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
10952|Mackunda Formation|69946|4|Described|p23, p26-28, p57, p94, p123|Late Cretaceous|Early Cretaceous|Vine and Day (1965). Type section is at the headwaters of Mackunda Creek on Gnalta Station. 60 - 120m thick. Wireline log correlations.||||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Interbedded, partly calcareous very fine-grained sandstone, siltstone and shale. Locally, transgressive mudstone units are interbedded with shoreface sandstones.|
10952|Mackunda Formation|69947|6|Mentioned|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marginal marine deposits.||||||
10952|Mackunda Formation|70821|5|Briefly described|p21, p33, p79-80|Late Cretaceous|Late Cretaceous|Eromanga Basin. Absent in the southern Thomson region. 30.5m thick in Mirintu 1 petroleum well. Hydrochemistry mentioned.||Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70823|5|Briefly described|p25-p27, p41, p43-p44,p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Age is minimum depositional age. Up to 200m thick.|c. 101 Ma|||Overlies the Allaru Formation and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|70836|6|Mentioned|p474|Albian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
10952|Mackunda Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlain by Winton Formation. Underlain by Mount Alexander Sandstone Member or Allaru Mudstone.||
10952|Mackunda Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p25,|Cenomanian|Albian|Eromanga Basin. Defined by Vine and Day (1965) who nominated the type section at the headwaters of Mackunda Creek on Gnalta Station. Hosts a major confined aquifer. Up to 120m thick. Dated on the basis of palynology and rare macrofossils.Sedimentology and palaeoenvironment are discussed. Spore-pollen zone is given in Ch5 p57.  See also Ch5 p23, Ch5 p26-p28, Ch5 p33, Ch5 p57, Ch5 p125, Ch6 p8, Ch6 p10, Ch7 p13.||||Conformably overlies the Allaru Mudstone and the Oodnadatta Formation. Conformably overlain by the Winton Formation.|Interbedded, partly calcareous, very fine-grained sandstone, siltstone and shale.|
10952|Mackunda Formation|71855|5|Briefly described|p27|||||||Overlies the Toolebuc Formation.||
10952|Mackunda Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Note that it also appears as a unit in the Neales River Group. Upper part: confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Oodnadatta FZ. Is overlain by Winton FZ.||
10952|Mackunda Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, calcareous; siltstone and shale.|
10952|Mackunda Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone, underlies the Winton Formation.||
10952|Mackunda Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Marginal marine.||||Underlain by Allura Mudstone. Underlain by and equivalent to Oodnadatta Formation.||
10952|Mackunda Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Allaru Mudstone. Equivalent to Winton Formation.||
10952|Mackunda Formation|73479|5|Briefly described|p156 Fig.2, p159-160, p166, p175|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97 Ma|||Overlies Allaru Mudstone, unconformably underlies Eyre Formation||
10967|Macrossan Gabbro|22847|3|Fully described|p 46|Early Devonian|Late Ordovician|||||||
10967|Macrossan Gabbro|23422|5|Briefly described|p214 Table 6.8|||||||||
10967|Macrossan Gabbro|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
10967|Macrossan Gabbro|23513|5|Briefly described|Map legend|Silurian|Ordovician|Palaeozoic Intrusive No. 452.||||||
10967|Macrossan Gabbro|42633|5|Briefly described|Table 1 P10|||Reserved as Macrossan Granodiorite.||||||
10967|Macrossan Gabbro|42750|2|Defined|p40|Early Silurian|Late Ordovician|||||||
10967|Macrossan Gabbro|43093|4|Described|Appendix 1|Early Silurian|Ordovician|Probable Middle Ordovician to Early Silurian age.||||||
10967|Macrossan Gabbro|43259|4|Described|Appendix 1,p48.|Late Silurian|Ordovician|||||||
10967|Macrossan Gabbro|43933|5|Briefly described|Map Legend|Devonian|Ordovician|||||||
10967|Macrossan Gabbro|43934|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
10967|Macrossan Gabbro|62521|5|Briefly described|p14-15|||Geological Province: Ravenswood Batholith. Comprises a series of discrete, and contiguous plutons - mainly of calcic plagioclase, hornblende, pyroxene; minor quartz. Mafic intrusive rocks.||||||21-DEC-07
10991|Maer Volcanics|33876|6|Mentioned|Map legend|Pleistocene|Pleistocene|Prob. Pleistocene||||||
10991|Maer Volcanics|33877|4|Described|p9|||Pleist. ?||||||
10991|Maer Volcanics|33880|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
10991|Maer Volcanics|34582|2|Defined|p530|Recent|Pleistocene|Pleistocene - Recent||||||
10991|Maer Volcanics|37607|6|Mentioned|Fig.6|||||||||
10991|Maer Volcanics|39445|5|Briefly described|Table 14|||||||||
10991|Maer Volcanics|45076|3|Fully described|p129|||P18 Refers Whitaker & Wilmot (1969).||||||
10991|Maer Volcanics|45087|5|Briefly described|p149|||Chemical analyses||||||
10991|Maer Volcanics|68553|6|Mentioned|Map legend|Quaternary|Quaternary|This unit, as well as the Barkers and Yates Creek Basalts; parts of the McBride and Nulla Basalt Groups, and unnamed basalt flows, are all mapped under the symbol, Qbn.||||||
10991|Maer Volcanics|69599|5|Briefly described|p641|Pleistocene|Pliocene|Willmott et al. (1973) and others. A small, remote lava-field province occurring as eight small islands in the NE Torres Strait.|3-1 Ma.||||Pyroclastic cones, tuffs and some lava flows; transitional to tholeiitic basalts and hawaiite.|
11011|Magnetic Island Granite|23422|5|Briefly described|p219 Table 6.12|||Of Woodstock Suite.||||||
11011|Magnetic Island Granite|23509|5|Briefly described|Map Legend||Permian|||||||
11011|Magnetic Island Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 140. I-Type.||||||
11011|Magnetic Island Granite|23893|5|Briefly described|p21|Permian|Permian|||||||
11011|Magnetic Island Granite|40607|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11011|Magnetic Island Granite|43259|4|Described|Appendix 1,p25.||Permian|||||||
11011|Magnetic Island Granite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
11011|Magnetic Island Granite|69593|5|Briefly described|p494|||Paluma Subprovince, Kennedy Igneous Association.||Woodstock Suite.||||
11011|Magnetic Island Granite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Magnetic Island.||||||
11018|Mail Change Limestone|22954|6|Mentioned|Fig3p9|||||||||
11018|Mail Change Limestone|23031|5|Briefly described|28|||Geol province Georgina Basin. Underlying unit V-Creek Limestone||||||
11018|Mail Change Limestone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|||||||
11018|Mail Change Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
11018|Mail Change Limestone|30479|6|Mentioned|Fig.6|||See also Fig.7. Stratigraphic relationships||||||
11018|Mail Change Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
11018|Mail Change Limestone|31396|6|Mentioned|Fig.3|||||||||
11018|Mail Change Limestone|33111|4|Described|p37|||Mention p27.||||||31-OCT-06
11018|Mail Change Limestone|34287|6|Mentioned|Fig.3|||||||||
11018|Mail Change Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
11018|Mail Change Limestone|34659|6|Mentioned|p221|||||||||
11018|Mail Change Limestone|35054|6|Mentioned|Table 23|||||||||
11018|Mail Change Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
11018|Mail Change Limestone|35139|4|Described|Table.2|||||||||
11018|Mail Change Limestone|35553|6|Mentioned|p175|||Appendix containing description of Agnostid localities.||||||
11018|Mail Change Limestone|37572|4|Described|p158|||See also Fig.7||||||
11018|Mail Change Limestone|38446|6|Mentioned|Table 23|||||||||
11018|Mail Change Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||31-OCT-06
11018|Mail Change Limestone|39690|6|Mentioned|Table 1|||||||||
11018|Mail Change Limestone|40686|5|Briefly described|p407|||||||||
11018|Mail Change Limestone|40856|6|Mentioned|Fig.23.6|||||||||
11018|Mail Change Limestone|41129|6|Mentioned|Fig.8|||||||||
11018|Mail Change Limestone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
11018|Mail Change Limestone|41388|6|Mentioned|Fig.2|||||||||
11018|Mail Change Limestone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
11018|Mail Change Limestone|44205|14|Not recorded|p51,155|||See also Lexicon.||||||
11018|Mail Change Limestone|44210|2|Defined|map,Tb.2,p13,14||Middle Cambrian|||||||
11018|Mail Change Limestone|44211|2|Defined|p101-107|||Overlain by Split Rock Sandstone and rests on V-Creek Limestone. Restricted to Undilla Basin.||||||
11018|Mail Change Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
11018|Mail Change Limestone|44275|14|Not recorded|Map Legend|||||||||
11018|Mail Change Limestone|44920|14|Not recorded|Map Legend,Sheet 2||Middle Cambrian|||||||
11018|Mail Change Limestone|45012|14|Not recorded|p338|||Fauna.||||||
11018|Mail Change Limestone|45052|3|Fully described|p94|||M.Camb.||||||
11018|Mail Change Limestone|45054|6|Mentioned|p6|||Fossil locality||||||
11018|Mail Change Limestone|45079|5|Briefly described|p34|||Cambrian age.||||||
11018|Mail Change Limestone|47058|6|Mentioned|p134|||||||||
11018|Mail Change Limestone|48906|14|Not recorded|Tb.1|||||||||
11018|Mail Change Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation.  Geological Province: eastern Georgina Basin.||||||31-OCT-06
11018|Mail Change Limestone|62791|6|Mentioned|p239|Middle Cambrian|Middle Cambrian|Source of the Type species of Treptotreta jucunda Henderson & MacKinnon 1981; Middle Cambrian (Goniagnostus nathorsti Biozone).||||||
11018|Mail Change Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
11018|Mail Change Limestone|64068|5|Briefly described|p62, 64, 225|||Eastern Georgina Basin. Correlated with Arthur Creek Formation, Roaring Siltstone, Devoncourt Limestone.||||||
11018|Mail Change Limestone|64443|6|Mentioned|p41|||Correlative of Ranken Limestone, Camooweal Dolostone.||||||
11018|Mail Change Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies V-Creek Limestone. Is overlain by Split Rock Sandstone.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules|
11018|Mail Change Limestone|69443|5|Briefly described|p28:16, 24-25|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Ranken Limestone and Camooweal Dolostone.||12-JUL-16
11018|Mail Change Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
11018|Mail Change Limestone|69591|4|Described|p87-88, p90, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Up to 30m thick. Contains abundant brachiopods and rare trilobites. Supratidal or high intertidal deposits. Coeval with Camooweal Dolostone and upper Age Creek Formation.||Narpa Group.||Conformably overlies V Creek Limestone. Is overlain by and grades laterally into Split Rock Sandstone.|Blue-grey and yellow mottled, thick-bedded, fine muddy limestone; includes microbial firm ground in upper shoreface settings and ephemeral evaporite horizons.|
11018|Mail Change Limestone|70380|5|Briefly described|p757|Cambrian|Cambrian|Eastern Georgina Basin. The cyclic pattern of deposition, interpreted as parasequences, is comparable with the Briggs Member of Oolloo Dolostone (Daly Basin).|||||Contains cycles of alternating limestone (<2m thick) and calcareous siltstone interbeds (up to 8m thick).|
11018|Mail Change Limestone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stage: Undillan.||of Narpa Group.||||
11018|Mail Change Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
11018|Mail Change Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies V-Creek Limestone, underlies Split Rock Sandstone|Limestone.|
11031|Main Range Volcanics|22601|6|Mentioned|405|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|23799|3|Fully described|p54, p9 Tb. 1|Early Miocene|Late Oligocene|Age: 25-19.4Ma (K/Ar, Webb et al, 1967).  Unconformably overlie Sugarloaf Mets., Cressbrook Gp., Tarong beds and Woogaroo Subgroup.  Max. thickness: ~1000m.  Geological Province: Main Range-Lamington Volcanic Province.||||||
11031|Main Range Volcanics|23800|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
11031|Main Range Volcanics|24560|5|Briefly described|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|29720|6|Mentioned|p80|||||||||
11031|Main Range Volcanics|30303|6|Mentioned|p322|||Overlies Cressbrook Group||||||
11031|Main Range Volcanics|31132|6|Mentioned|p148|||Refers Webb et al. (1967)||||||
11031|Main Range Volcanics|31273|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|32103|6|Mentioned|p406|||||||||
11031|Main Range Volcanics|32491|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|32492|6|Mentioned|Map legend|Miocene|Miocene|||||||
11031|Main Range Volcanics|32797|6|Mentioned|p17|||||||||
11031|Main Range Volcanics|32912|5|Briefly described|p157|||See also Table 1||||||
11031|Main Range Volcanics|32924|6|Mentioned|p111|||Refers Stevens (1965)||||||
11031|Main Range Volcanics|33091|5|Briefly described|p7|||Stratigraphy||||||
11031|Main Range Volcanics|33290|4|Described|p38|||||||||
11031|Main Range Volcanics|33381|4|Described|p121|||Tertiary. See also p123.||||||24-SEP-22
11031|Main Range Volcanics|33476|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|33705|6|Mentioned|p45|||||||||
11031|Main Range Volcanics|33751|6|Mentioned|p149|||||||||
11031|Main Range Volcanics|33766|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|34507|6|Mentioned|p87|||||||||
11031|Main Range Volcanics|35101|3|Fully described|p58|||||||||
11031|Main Range Volcanics|36579|6|Mentioned|p447|||||||||
11031|Main Range Volcanics|36779|6|Mentioned|p8|||||||||
11031|Main Range Volcanics|36926|6|Mentioned|p165|||||||||
11031|Main Range Volcanics|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|37376|6|Mentioned|p491|||||||||
11031|Main Range Volcanics|37389|6|Mentioned|p54|||||||||
11031|Main Range Volcanics|37391|6|Mentioned|p26|||||||||
11031|Main Range Volcanics|37435|6|Mentioned|Fig.2|||||||||
11031|Main Range Volcanics|38205|2|Defined|p89|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
11031|Main Range Volcanics|39071|6|Mentioned|p344|||||||||
11031|Main Range Volcanics|39445|5|Briefly described|Table 14|||||||||
11031|Main Range Volcanics|39998|6|Mentioned|p192|||||||||
11031|Main Range Volcanics|40475|5|Briefly described|p9|||Also Mention on P5.||||||
11031|Main Range Volcanics|40485|6|Mentioned|Fig.1|||||||||
11031|Main Range Volcanics|40486|6|Mentioned|p84|||||||||
11031|Main Range Volcanics|40488|6|Mentioned|p92|||||||||
11031|Main Range Volcanics|40513|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|40623|5|Briefly described|p72|||||||||
11031|Main Range Volcanics|40734|6|Mentioned|p65|||||||||
11031|Main Range Volcanics|41906|6|Mentioned|p40|||||||||
11031|Main Range Volcanics|42041|6|Mentioned|p221|||||||||
11031|Main Range Volcanics|42485|4|Described|p264|||||||||
11031|Main Range Volcanics|42525|5|Briefly described|Map legend|Miocene|Oligocene|||||||
11031|Main Range Volcanics|43003|5|Briefly described|p169|||||||||
11031|Main Range Volcanics|43007|5|Briefly described|p258|||||||||
11031|Main Range Volcanics|43100|5|Briefly described|p49|||||||||
11031|Main Range Volcanics|43150|5|Briefly described|Map Legend||Tertiary|||||||
11031|Main Range Volcanics|44782|2|Defined|p39-42,44-46,49,51,||Tertiary|Pl.1.||||||
11031|Main Range Volcanics|44783|14|Not recorded|p2|||||||||
11031|Main Range Volcanics|44784|4|Described|p11,map 3||Tertiary|||||||
11031|Main Range Volcanics|44786|14|Not recorded|p193-202||Miocene|Early Miocene||||||
11031|Main Range Volcanics|44813|14|Not recorded|p80,82,83,85,89||Tertiary|Contains early Miocene flows. 22-24 Ma.||||||
11031|Main Range Volcanics|44818|6|Mentioned|p276|||||||||
11031|Main Range Volcanics|44923|5|Briefly described|Map Legend||Tertiary|||||||
11031|Main Range Volcanics|45087|5|Briefly described|p114|||Chemical analyses||||||
11031|Main Range Volcanics|45110|6|Mentioned|Table 21|||||||||
11031|Main Range Volcanics|48917|4|Described|p37|||See also p7. Refers Stevens (1966)||||||24-SEP-22
11031|Main Range Volcanics|50320|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|50322|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies: Walloon Coal Measures, Koukandowie Formation.||||||
11031|Main Range Volcanics|50384|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|50631|5|Briefly described|Map Legend|Tertiary|Tertiary|Basalt, minor trachyte.||||||
11031|Main Range Volcanics|60077|5|Briefly described|Map legend|Tertiary|Tertiary|Basalt, dolerite, minor shale, siltstone, diatomite.||||||
11031|Main Range Volcanics|60370|5|Briefly described|Map Legend|Tertiary|Tertiary|Olivine basalt; sandstone, shale, siltstone, conglomerate, diatomite.||||||
11031|Main Range Volcanics|60371|5|Briefly described|Map Legend|Tertiary|Tertiary|Olivine basalt; sandstone, shale, siltstone, conglomerate, diatomite, locally intercalated with basalt flows.||||||
11031|Main Range Volcanics|61007|5|Briefly described|p300|Early Miocene|Early Miocene|Extensive extruded basalts.||||||
11031|Main Range Volcanics|61310|6|Mentioned|p22|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|63731|5|Briefly described|Map legend||Tertiary|Rhyolite (intrusive plug). Olivine basalt lava; minor mudstone and sandstone.||||||12-DEC-07
11031|Main Range Volcanics|63748|5|Briefly described|p22, p23-24|Early Miocene|Late Oligocene|Unconformably overlie Marburg Subgroup in the Warwick area; also overlies Walloon C.M. Geological province: Lamington-Main Range Volcanics Province. Massive, fine-grained olivine basalt, occurring mainly as flows. Also mentioned on p50.||||||07-FEB-11
11031|Main Range Volcanics|65003|4|Described|p7,p9, p22||Miocene|Of Clarence-Moreton Basin.|||||Olivine basalt, tuff, agglomerate, dolerite; minor shale, siltstone, and diatomite.|30-MAR-12
11031|Main Range Volcanics|67402|6|Mentioned|p258|||Tarong Basin.||||||
11031|Main Range Volcanics|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran, Gin Gin and Mount Runsome Basalts; Minerva Hills, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
11031|Main Range Volcanics|68679|5|Briefly described|p322-323, p396, p455|Neogene|Paleogene|Tertiary.||||Unconformably overlies Maronghi Creek beds, Sugarloaf Metamorphics and Chahpingah Meta-Igneous Complex.||
11031|Main Range Volcanics|68901|6|Mentioned|p8 Fig. iii|Paleogene|Paleogene|||||||27-SEP-18
11031|Main Range Volcanics|69594|6|Mentioned|p545|Cenozoic|Cenozoic|Clarence-Moreton Basin.||||||
11031|Main Range Volcanics|69599|5|Briefly described|p584, p598|||Near Maidenwell, diatomite is commercially mined. An extensive duricrust developed on this (and other) units.|||||Contains a sedimentary assemblage of sandstone, shale, siltstone, conglomerate, tuffaceous sediments and diatomite interbedded with basalt.|
11031|Main Range Volcanics|69793|6|Mentioned|p1113 Fig.3|Cenozoic|Cenozoic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
11031|Main Range Volcanics|72297|5|Briefly described|p726|Miocene|Oligocene|Basalt lavas dammed local drainages, producing lakes in which diatomite deposits accumulated (eg Mount Sylvia, Maidenwell).|||||Basalt.|
11031|Main Range Volcanics|72298|6|Mentioned|p797|Cenozoic|Cenozoic|Underlies unconsolidated Quaternary alluvium which supplies most of the groundwater in the Lockyer Valley.||||||
11031|Main Range Volcanics|73113|5|Briefly described|p. 7, 22-23, 26, 41, 44-45, 48, 88...|||Surat Basin. Partial aquifer. More locations: p. 98, 116, 118-122, 140, 146, 151-152, 158, 160-161, 171-172.||||||
11031|Main Range Volcanics|73200|5|Briefly described|p532-p533, p539 Fig.11, p541, p543|Early Miocene|Late Oligocene|Abbreviated to MRV on p533 Fig.4 [and MRB on p542 Fig.14?].||||Overlies the Walloon Coal Measures.|Olivine basalt with pyroclastic rocks.|
11031|Main Range Volcanics|73450|4|Described|p90-95|Chattian|Chattian|Grouped into northern and southern subunits. In the southwest, there is a thick (up to 900 m) sequence of lavas, pyroclastic rocks and minor conglomerate that thins westward. In the southeast, erosion has exposed a related group of mafic and felsic shallow-level intrusive bodies in the Fassifern Valley. Mafic and felsic divisions are not in use on the current geological coverage. Felsic flows are locally glassy/devitrified, porphyritic or vesicular. Yielded various K-Ar and Ar-Ar ages averaging ca 26 Ma (or younger).|ca 26 Ma||Cooby Trachyte Member, Nutgrove Rhyolite Member||Includes metaluminous and peralkaline trachyte to rhyolite flows, breccia, tuffs and ignimbrites.|
11049|Makbat Sandstone|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11049|Makbat Sandstone|33111|6|Mentioned|p38|||||||||
11049|Makbat Sandstone|33900|6|Mentioned|p19|||||||||
11049|Makbat Sandstone|35074|6|Mentioned|Fig.2|||||||||
11049|Makbat Sandstone|35121|6|Mentioned|Map legend|Early Cambrian|Adelaidean|||||||
11049|Makbat Sandstone|35139|4|Described|Table.2|||||||||
11049|Makbat Sandstone|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11049|Makbat Sandstone|37862|6|Mentioned|p582|||||||||
11049|Makbat Sandstone|38350|6|Mentioned|p11|||||||||
11049|Makbat Sandstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11049|Makbat Sandstone|39445|5|Briefly described|Table 3|||?Carpentarian See p55.||||||02-APR-07
11049|Makbat Sandstone|40840|6|Mentioned|Map legend|||||||||
11049|Makbat Sandstone|42565|5|Briefly described|Table 1 P5|||||||||
11049|Makbat Sandstone|44271|2|Defined|p40,41|||||||||
11049|Makbat Sandstone|44275|14|Not recorded|Map Legend|||||||||
11049|Makbat Sandstone|44276|2|Defined|p12,14,18,Tb.1,map|||||||||
11049|Makbat Sandstone|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
11049|Makbat Sandstone|44290|2|Defined|p439||Neoproterozoic|||||||
11049|Makbat Sandstone|44361|14|Not recorded|Map Legend||Neoproterozoic|||||||
11049|Makbat Sandstone|44362|4|Described|p9,Tb.1||Neoproterozoic|||||||
11049|Makbat Sandstone|44920|14|Not recorded|Map Legend,Sheet 4|Early Cambrian|Adelaidean|||||||
11049|Makbat Sandstone|44989|2|Defined|p.122-3|||Tb.II. On many pages. (F54-6,10).||||||
11049|Makbat Sandstone|45052|4|Described|p74|||U.Prot.||||||
11049|Makbat Sandstone|45161|5|Briefly described|p26|||||||||
11049|Makbat Sandstone|45166|5|Briefly described|p17|||||||||
11049|Makbat Sandstone|45287|14|Not recorded|p.223,226|Paleozoic|Neoproterozoic|U. Prot - Palae.||||||07-NOV-08
11049|Makbat Sandstone|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
11049|Makbat Sandstone|46960|6|Mentioned|p216|||||||||
11049|Makbat Sandstone|46962|4|Described|Table 1|||See also Fig.3.||||||
11049|Makbat Sandstone|46996|6|Mentioned|p273|||||||||
11049|Makbat Sandstone|49009|6|Mentioned|p22|||||||||
11049|Makbat Sandstone|49041|5|Briefly described|Table 1|||||||||
11049|Makbat Sandstone|50100|5|Briefly described|p13 Fig.4, p19|Statherian|Statherian|Mainly quartzose to feldspathic sandstone with local basal conglomerates containing volcanic detritus.  Overlies the Leichhardt Volcanics and Wills Creek Granite.  Geological Province: Kalkadoon-Ewen Province.||||||
11049|Makbat Sandstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite, siltstone, basal conglomerate.||||||
11049|Makbat Sandstone|64250|6|Mentioned|p8|||Omitted from stratigraphic chart because of limited exposure.||||||
11049|Makbat Sandstone|65396|6|Mentioned|p174|||Southern Kalkadoon-Leichhardt Belt. Small unit with limited exposure.||||(Possibly) Correlated with Ballara Quartzite.||
11049|Makbat Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p107|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Calvert Superbasin.|||||Feldspathic arenite, quartz arenite, greywacke, siltstone; minor shale, conglomerate.|
11049|Makbat Sandstone|69591|5|Briefly described|p39-40, p55|||Duchess area, Kalkadoon-Leichhardt Domain. Age uncertain; considered part of the Prize and Gun Supersequences.|||||Feldspathic arenite, quartz arenite, greywacke, siltstone; minor shale, conglomerate.|
11082|Malchi Formation|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Crm].  Silicified mudstone, lithic sandstone, oolitic limestone, conglomerate.||||||
11082|Malchi Formation|31657|5|Briefly described|p94|||See also P101. U.Tournaisian to U.Visean||||||
11082|Malchi Formation|31659|4|Described|p52, p53|Visean|Tournaisian|Of the Rockhampton Group. Overlain by the Lion Creek Limestone and underlain by the basal unit, Gudman Oolite. Constitutes the bulk of the group.||||||09-JUN-09
11082|Malchi Formation|32866|6|Mentioned|p10|||Fossil content||||||
11082|Malchi Formation|32868|6|Mentioned|p208,Fig.7|||||||||
11082|Malchi Formation|36528|6|Mentioned|p172|||||||||
11082|Malchi Formation|38406|6|Mentioned|p11|||||||||
11082|Malchi Formation|39445|5|Briefly described|Table 6|||||||||
11082|Malchi Formation|41576|4|Described|Table 1|||||||||
11082|Malchi Formation|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
11082|Malchi Formation|41826|6|Mentioned|p325|||||||||
11082|Malchi Formation|42002|6|Mentioned|p94|||||||||
11082|Malchi Formation|42547|4|Described|p49|||||||||
11082|Malchi Formation|42583|5|Briefly described|p65|||||||||
11082|Malchi Formation|44360|14|Not recorded|p30,31||Early Carboniferous|Unit of Rockhampton Group.||||||
11082|Malchi Formation|44379|14|Not recorded|p15|||Ref. to Fleming 1967||||||
11082|Malchi Formation|44388|2|Defined|p113-115|Visean|Tournaisian|Overlies Gudman Oolite. Overlain by Lion Creek Limestone. (late Tournaisian - Visean)||||||
11082|Malchi Formation|46803|6|Mentioned|p143|||See also Fig. 4||||||
11082|Malchi Formation|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Rockhampton Group.  Includes: Cargoogie Oolite Member.||||||17-MAY-04
11082|Malchi Formation|60557|5|Briefly described|p32|||Part of the Bouldercomb Complex (ie. the Bouldercombe Igneous Complex).||||||09-JUN-05
11082|Malchi Formation|61557|5|Briefly described|p878.|Early Carboniferous|Early Carboniferous|||||Overlies the Gudman Formation.|A thick sequence of mudstone, siltstone, and feldsarenite turbidites.|
11082|Malchi Formation|68008|5|Briefly described|p90, p93, p95, p594|Early Carboniferous|Early Carboniferous|Fleming (1967). Not reliably recognised outside the Stanwell area. Detailed facies description.||Rockhampton Group.|Cargoogie Oolite Member.|(An equivalent) overlies Gudman Oolite (equivalent).||
11082|Malchi Formation|68679|5|Briefly described|p340|||Fleming (1967).||Rockhampton Group.|Cargoogie Oolite Member.|||
11082|Malchi Formation|70050|5|Briefly described|p318, p325, p328, p362-367|Tournaisian|Tournaisian|Lion Creek and Ridgelands blocks, Rockhampton area. Contains Cionodendron coral fossils (illustrations and systematic palaeontology), including the oldest representative of Cionondendroninae.|||Cargoogie Oolite Member.||Siltstone; includes fossiliferous limestone beds.|
11088|Maleny Lavas|36806|6|Mentioned|Table 4|||||||||
11088|Maleny Lavas|38310|6|Mentioned|p237|||||||||
11088|Maleny Lavas|63187|6|Mentioned|p108|Early Miocene||||||||
11201|Mant Basalt|22857|5|Briefly described|p262|Early Permian|Early Permian|Geological Province: Gympie Terrane.||||||
11201|Mant Basalt|22864|6|Mentioned|p262||Early Permian|||||||
11201|Mant Basalt|24382|5|Briefly described|Map legend|Permian|Permian|Parent: Gympie Group.||||||14-AUG-08
11201|Mant Basalt|41736|2|Defined|p118|Early Permian||Reserved as Mant. See also Fig.1||||||
11201|Mant Basalt|42054|6|Mentioned|p272|||||||||
11201|Mant Basalt|43017|5|Briefly described|Fig.3,p375|||||||||
11201|Mant Basalt|63821|4|Described|p17, p39|Early Permian|Early Permian|Basal unit of Gympie Group. Geological Province: Gympie Province. Consists of altered basaltic pillow lavas, amygdaloidal basalts and minor tuff and pyroclastic breccias. Interpreted as seafloor basalt, probably part of an oceanic arc.||||||07-FEB-11
11201|Mant Basalt|68679|5|Briefly described|p370-371|Permian|Mississippian|Northern Gympie Province. Crops out in anticlinal axes around Gigoomgan and western slopes of the Urah Range. 180m thick.||||Correlated with Highbury Volcanics.|Altered basaltic pillow lavas, amygdaloidal basalts and minor tuff and pyroclastic breccias.|
11201|Mant Basalt|73303|5|Briefly described|p61 Fig.2, p62, p64|Early Permian|Early Permian|New England Orogen. Gympie Terrane, northern. Contains evidence of subaqueous deposition. Considered to be the same lithological unit as the Highbury Basalt. Included as a member of the Kolbar Formation (p64).||Kolbar Formation||At base of Kolbar Formation.|Basaltic unit.|
11207|Mantuan Productus Bed|24069|5|Briefly described|p284|Permian|Permian|Of Tinowon Formation. Geological Province: Surat Basin.||||||
11207|Mantuan Productus Bed|24077|5|Briefly described|p410 Tb. 2|Late Permian|Late Permian|Of the Peawaddy Formation.  Coquinitic shale, siltstone and sandstone (marine).  Max. thickness: 125m.  Geological Province: Bowen Basin.||||||
11207|Mantuan Productus Bed|29409|6|Mentioned|Table 1|||||||||
11207|Mantuan Productus Bed|29721|6|Mentioned|Table 65|||||||||
11207|Mantuan Productus Bed|30153|6|Mentioned|p151|||||||||
11207|Mantuan Productus Bed|30341|6|Mentioned|p136|||Upper Permian age||||||
11207|Mantuan Productus Bed|30545|6|Mentioned|Fig.2|||Kazanian||||||
11207|Mantuan Productus Bed|32578|5|Briefly described|Table 1|||Permian||||||
11207|Mantuan Productus Bed|32689|6|Mentioned|Fig.2|||Refers Power (1967)||||||
11207|Mantuan Productus Bed|32945|6|Mentioned|p81|||See also P91 & Fig.3. Permian||||||
11207|Mantuan Productus Bed|33059|4|Described|Table 1|||U.Perm.||||||
11207|Mantuan Productus Bed|33366|6|Mentioned|Fig.3|||Perm.||||||
11207|Mantuan Productus Bed|33701|6|Mentioned|Fig.1|||Kazanian.||||||
11207|Mantuan Productus Bed|34099|6|Mentioned|p10|||||||||
11207|Mantuan Productus Bed|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
11207|Mantuan Productus Bed|36241|6|Mentioned|p125|||||||||
11207|Mantuan Productus Bed|39212|5|Briefly described|p11|||||||||
11207|Mantuan Productus Bed|39263|6|Mentioned|p142|||||||||
11207|Mantuan Productus Bed|41639|6|Mentioned|p7|||||||||
11207|Mantuan Productus Bed|41666|6|Mentioned|p25|||||||||
11207|Mantuan Productus Bed|42856|5|Briefly described|Fig.9 P642|||||||||
11207|Mantuan Productus Bed|43474|14|Not recorded|fig.1,opp.p6,p39,52,|||p86||||||
11207|Mantuan Productus Bed|43544|14|Not recorded|p319|||||||||
11207|Mantuan Productus Bed|43879|14|Not recorded|p254||Permian|Springsure area.||||||
11207|Mantuan Productus Bed|43883|14|Not recorded|p18 Fig.4-3|||||||||
11207|Mantuan Productus Bed|43977|14|Not recorded|p577,580|||See also Lexicon.||||||
11207|Mantuan Productus Bed|43987|14|Not recorded|p267,270|||||||||
11207|Mantuan Productus Bed|43990|6|Mentioned|Map Legend|||Mention in map legend.||||||
11207|Mantuan Productus Bed|44081|14|Not recorded|p30,53-56|||Described in French.||||||
11207|Mantuan Productus Bed|44085|2|Defined|Op.p4,8,10,11,16,map|||||||||
11207|Mantuan Productus Bed|44095|14|Not recorded|p285|||||||||
11207|Mantuan Productus Bed|44103|2|Defined|p212,214-215|||Overlies Colinlea Formation.||||||
11207|Mantuan Productus Bed|44169|14|Not recorded|Tb.1|||||||||
11207|Mantuan Productus Bed|44170|14|Not recorded|Tb.1,p11|||Included in Peawaddy Formation.||||||
11207|Mantuan Productus Bed|44172|14|Not recorded|p1327-8,1333,1337,||Kazanian|p1343,Fig.2,Tb.1.||||||
11207|Mantuan Productus Bed|44173|14|Not recorded|p112 (fig.2)|||||||||
11207|Mantuan Productus Bed|44347|14|Not recorded|p77|||||||||
11207|Mantuan Productus Bed|44348|14|Not recorded|p56|||||||||
11207|Mantuan Productus Bed|44349|14|Not recorded|p64|||||||||
11207|Mantuan Productus Bed|44421|14|Not recorded|p8,map||Permian|||||||
11207|Mantuan Productus Bed|44422|14|Not recorded|p150,152|||Mantuan Productus Bed + "Dry Creek Shale" = Peawaddy Formation.||||||
11207|Mantuan Productus Bed|44424|14|Not recorded|p293-301|||At top of Peawaddy Formation.||||||
11207|Mantuan Productus Bed|44488|14|Not recorded|p48|||||||||
11207|Mantuan Productus Bed|44489|14|Not recorded|p71,72|||||||||
11207|Mantuan Productus Bed|44490|14|Not recorded|p48|||||||||
11207|Mantuan Productus Bed|44618|14|Not recorded|p517,518||Permian|Is upper part of Peawaddy Formation. Top is correlated with top of Arcturus gas sands||||||
11207|Mantuan Productus Bed|46849|6|Mentioned|p192|||||||||
11207|Mantuan Productus Bed|48626|4|Described|p1,3,22,24-5,30-2,51||Permian|p55,58,93||||||
11207|Mantuan Productus Bed|48630|14|Not recorded|p1,4,6,18-20,Pls.1,2|||||||||
11207|Mantuan Productus Bed|48831|14|Not recorded|p.18,41|||||||||
11207|Mantuan Productus Bed|48847|14|Not recorded|p10,Pl.2,p1|||||||||
11207|Mantuan Productus Bed|48900|6|Mentioned|p23|||||||||
11207|Mantuan Productus Bed|60330|5|Briefly described|p261 Fig.2|Kazanian|Kazanian|||||||
11207|Mantuan Productus Bed|63713|5|Briefly described|p1507 Fig.2, p1528|Capitanian|Capitanian|Roma Shelf, Bowen Basin. Shown as part of Tinowon Formation. Appears as Mantuan Productus Beds in Fig.2. Well-log correlation.||||||
11207|Mantuan Productus Bed|73625|5|Briefly described|p15, 18, 20-21, 24|Permian|Permian|Hill (1957); formalized by Tweedale (1960). The topmost part of the Peawaddy Formation. Appears also as Mantuan Productus Beds on p18.|c.254.5 Ma.|||Is overlain by Black Alley Shale.|Bioturbated, shell fossil-bearing and gravel-rich sandstones. Contains concentrations (locally coquinite beds) of invertebrate shells, esp. the productid Echinalosia ovalis.|
11215|Manuka Subgroup|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Cretaceous|Late Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
11215|Manuka Subgroup|29591|6|Mentioned|p69|||||||||
11215|Manuka Subgroup|39445|6|Mentioned|Table 11|||||||||
11215|Manuka Subgroup|63979|5|Briefly described|p53|||Of Rolling Downs Group. Includes Mackunda and Winton Formations.||||||07-FEB-11
11215|Manuka Subgroup|69457|5|Briefly described|p41:6, 11-13|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga Basin.||Rolling Downs Group.|Mackunda and Winton Formations.|Overlies Wilgunya and Marree Subgroups.||12-JUL-16
11215|Manuka Subgroup|69673|6|Mentioned|p156||||||Includes Mackunda Formation, Winton Formation|Overlies Wilgunya Subgroup||
11255|Marburg Subgroup|12597|5|Briefly described|p491, p492 Tb.1, p494, p501|Bathonian|Pliensbachian|Clarence-Moreton Basin. Appears as Marburg Formation on p496. Contains thin coal seams of no apparent commercial value in its lower parts.||Unit in Bundamba Group.|Includes Gatton Sandstone and Koukandowie Formation.|||
11255|Marburg Subgroup|13516|5|Briefly described|p159 fig 8|Jurassic|Jurassic|From Clarence-Moreton Basin.||Of Bundamba Group|Includes Gatton Sandstone, Koukandowie Formation|||
11255|Marburg Subgroup|22857|5|Briefly described|p318-9, p548 App. 1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Bundamba Group. Max. thickness: 1200m. Geological Province: Clarence-Moreton Basin. See also p548 App.1 Tb.A1.12.||||||
11255|Marburg Subgroup|22865|4|Described|p318,Fig22.9p317|||||||||
11255|Marburg Subgroup|23799|3|Fully described|p47|Early Jurassic|Early Jurassic|See also p10 Tb. 1.  Formerly Marburg Formation.  Currently defined to include Gatton Sandstone and Koukandowie Formation forming upper part of the Bundamba Group.  Overlies Woogaroo Group.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group.||||||11-DEC-07
11255|Marburg Subgroup|23811|5|Briefly described|Map Legend|||Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|23812|5|Briefly described|p33 Fig.6|||Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||27-AUG-08
11255|Marburg Subgroup|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Bundamba Group.||||||
11255|Marburg Subgroup|41631|4|Described|p14|||See also Fig.2 and Fig.4.||||||
11255|Marburg Subgroup|42248|1|Redefined|App.1 p409|Early Jurassic||Redefined from Marburg Formation.||||||27-SEP-18
11255|Marburg Subgroup|42463|6|Mentioned|Fig.3 P170|||||||||
11255|Marburg Subgroup|42869|5|Briefly described|Fig.2 P32|||||||||
11255|Marburg Subgroup|42894|5|Briefly described|Fig.1 P20|||||||||
11255|Marburg Subgroup|42951|5|Briefly described|Fig.11|||Of Bundamba Group.||||||11-DEC-07
11255|Marburg Subgroup|43150|5|Briefly described|Map Legend||Jurassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
11255|Marburg Subgroup|43736|6|Mentioned|p3|||||||||
11255|Marburg Subgroup|44450|5|Briefly described|p27|||Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Bundamba Group.  Includes: Gatton Sandstone, Koukandowie Formation.||||||
11255|Marburg Subgroup|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group. Geological Province: Moreton Basin||||||
11255|Marburg Subgroup|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Sandstone, conglomerate, siltstone, claystone, minor coal and basalt.||||||
11255|Marburg Subgroup|60281|5|Briefly described|p22, p27, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Bundamba Group. Includes the Gatton Sandstone and Koukandowie Formation.  Equivalent to the Evergreen Formation and Hutton Sandstone of the Surat Basin.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60993|3|Fully described|p17, p6 Fig. 2|||Of the Bundamba Group. Redefinition of constituent units within the group. Conformably overlain by Walloon Coal Measures. Conformably overlies the Woogaroo Subgroup. Geol. Prov: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60995|4|Described|p62-63, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Bundamba Gp. Formerly referred to as the Marburg sequence ('formation', 'sandstone'). Geological Province: Clarence-Moreton Basin. Parts of the subgroup have been referred to as the Marburg sequence.||||||
11255|Marburg Subgroup|60996|5|Briefly described|p113 Fig. 64|||Includes the Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60997|5|Briefly described|p138, p142 Fig. 4|Bathonian|Sinemurian|Contains quartzo-feldspathic to quartz-lithic sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2.||||||
11255|Marburg Subgroup|60998|5|Briefly described|p144, p146 Fig. 2|||Includes the Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60999|5|Briefly described|p164|Early Jurassic||Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|61004|5|Briefly described|p230|||Of the Bundamba Group. Includes the Gatton Sandstone and Koukandowie Formation. Contains high vitrinite and relatively low liptinite contents. Geological Province: Clarence-Moreton Basin.||||||08-MAY-13
11255|Marburg Subgroup|61006|5|Briefly described|p277, p278 Fig. 2|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|61310|5|Briefly described|p14 Fig. C5|||Part of Bundamba Group (as Marburg Subgroup)? Or overlies the Bundamba Group? Overlain by Walloon Coal Measures. Geological Province: Clarence-Moreton Basin||||||
11255|Marburg Subgroup|63729|5|Briefly described|Map legend|Jurassic|Jurassic|Underlies Walloon Coal Measures; upper section interfingers with Kumbarilla beds. Medium- to coarse-grained quartzose and quartzofeldspathic sandstone and conglomerate.||||||11-DEC-07
11255|Marburg Subgroup|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Includes the Gatton Sandstone and Walloon Coal Measures.||||||12-DEC-07
11255|Marburg Subgroup|63732|5|Briefly described|Map legend||Jurassic|Fine- to medium-grained, highly porphyritic (titanite-biotite-) hornblende diorite; with numerous phenocrysts of plagioclase to ~1.5cm and brown hornblende to ~5mm.||||||
11255|Marburg Subgroup|63733|5|Briefly described|Map legend|Jurassic|Jurassic|Medium to coarse-grained quartzose and quartzofeldspathic sandstone and conglomerate.||||||
11255|Marburg Subgroup|63748|6|Mentioned|p19, p21-22|Jurassic|Jurassic|Upper part of Bundamba Group. Includes Gatton Sandstone. Overlies the Woogaroo Subgroup. In Warwick area, unconformably overlain by Main Range Volcanics, conformably overlain by Walloon Coal Measures.  See also p7 Fig. 3.||||||07-FEB-11
11255|Marburg Subgroup|64289|5|Briefly described|p6 Fig. 2, p17. p18|Middle Jurassic|Early Jurassic|Of the Woogaroo Subgroup (Bundamba Group). Includes Gatton Sandstone and Koukandowie Formation (and its two members). Geological province: Clarence-Moreton Basin. Hosts Plensbachian-Toarcian flora; fragmentary vertebrate remains occur also.||||||07-FEB-11
11255|Marburg Subgroup|64665|5|Briefly described|p53 Fig.2, p59.|Middle Jurassic|Early Jurassic|Clarence-Moreton and Southern Nambour Basins. Includes thin, uneconomic coals.||Upper unit in Bundamba Group.|Includes Gatton Sandstone, Koukandowie Formation, the upper part of Landsborough Sandstone, and Brighton beds.|Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|64856|5|Briefly described|p86|||Moreton Basin unit. Hutton Sandstone is laterally continuous into the upper part of this Subgroup. Shown as Marburg Sub-Group.|| ||||31-JAN-13
11255|Marburg Subgroup|65388|6|Mentioned|p213|||Moreton Basin.  Lower part laterally continuous with Evergreen Formation, Surat Basin.||||||
11255|Marburg Subgroup|67402|6|Mentioned|p187|||Clarence-Moreton Basin.||Bundamba Group|Includes the Gatton Sandstone and the Koukandowie Formation.|||
11255|Marburg Subgroup|68135|6|Mentioned|p64|||Lowood area, Clarence-Moreton Basin. Contains the late Early to early Middle Jurassic labyrinthodont amphibian, Austropelor, Longman, 1941.||||||
11255|Marburg Subgroup|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Bundamba Group, the Woogaroo Subgroup, and Landsborough Sandstone, are all mapped under the symbol, RJb.||Unit in Bundamba Group.||||
11255|Marburg Subgroup|68679|5|Briefly described|p452-453, p455|Jurassic|Jurassic|||||Unconformably overlies the Eight Mile Creek, Condamine and Rhyolite Range beds.||
11255|Marburg Subgroup|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
11255|Marburg Subgroup|69594|5|Briefly described|p519, p535-536, p543-545, p547|||Clarence-Moreton Basin and southern Nambour Basin. Meandering stream deposits.||Bundamba Group.|Koukandowie Formation, Gatton Sandstone, Brighton beds.|Overlies Woogaroo Subgroup. Is overlain transitionally by Walloon Coal Measures. Part-equivalent to the Evergreen Formation and Hutton Sandstone.||
11255|Marburg Subgroup|69639|6|Mentioned|p192, p222|Jurassic|Jurassic|||||Overlies the Cullendore Granite.||
11255|Marburg Subgroup|69790|5|Briefly described|p1063 Fig.2, p1076|Middle Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Bundamba Group.|Includes Gatton Sandstone and Koukandowie Formation.|||
11255|Marburg Subgroup|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Bundamba Group.|Gatton Sandstone, Koukandowie Formation.|Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|71628|5|Briefly described|p15: 34, 70; p16-4|Jurassic|Jurassic|Clarence-Moreton Basin. Appears as Marburg Supergroup on p15-34.|||Koreelah Conglomerate Member.|Locally overlies Cullendore Syenogranite and units of the Stanthorpe Complex.||
11255|Marburg Subgroup|71805|5|Briefly described|p76|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||Bundamba Group|Includes the Gatton Sandstone and the Koukandowie Formation.|||15-MAY-19
11255|Marburg Subgroup|72297|5|Briefly described|p726, p746|||Clarence-Moreton Basin. Quarried near Warwick and Yangan: coarse sandstone for landscaping; fine for tiles, sculpture and building stone. Carbonaceous shales may form hydrocarbon source rocks.|||Heifer Creek Sandstone Member.||Fine to coarse sandstones.|
11255|Marburg Subgroup|72298|6|Mentioned|p798|||Permeable sandstone beds in this unit are groundwater aquifers in the Ma Ma Creek catchment (Lockyer Valley).||||||
11255|Marburg Subgroup|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||Underlies the Walloon Coal Measures.||
11255|Marburg Subgroup|73306|5|Briefly described|p566-567, 569-570|Jurassic|Jurassic|Clarence-Moreton Basin. It is displaced by several minor normal faults.||Bundamba Group.||Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|73570|5|Briefly described|p914|Early Jurassic|Early Jurassic|Clarence-Morton Basin. See also Marburg Group p915 Fig.4.|||Gatton Sandstone|||
11284|Mareeba Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|Early Permian S-type granite along the eastern side of Hodgkinson Province. Apatite fission track analyses are detailed.|279-262 Ma.|Unit in Whypalla Supersuite.||||
11284|Mareeba Granite|23423|6|Mentioned|p243|||||||||
11284|Mareeba Granite|23497|6|Mentioned|p33, 34|||||||||
11284|Mareeba Granite|23506|5|Briefly described|Map Legend||Early Permian|of Whypalla Supersuite. Age: 282+/-9Ma Rb-Sr.||||||
11284|Mareeba Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 300. S-Type.||||||
11284|Mareeba Granite|23616|5|Briefly described|p77||Early Permian|S-type Granite. Of Whypalla Supersuite. Hodgkinson Province.||||||
11284|Mareeba Granite|23856|5|Briefly described|p875|Early Permian|Early Permian|||||||
11284|Mareeba Granite|29605|6|Mentioned|p1|||||||||
11284|Mareeba Granite|29794|6|Mentioned|Fig.1|||||||||
11284|Mareeba Granite|29795|6|Mentioned|p273|||||||||
11284|Mareeba Granite|29796|6|Mentioned|Fig.1|||||||||
11284|Mareeba Granite|30505|5|Briefly described|p5|||See also P6,7,15. Permian age||||||
11284|Mareeba Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
11284|Mareeba Granite|31435|6|Mentioned|p17|||||||||
11284|Mareeba Granite|31832|6|Mentioned|Table 6|||||||||
11284|Mareeba Granite|32634|6|Mentioned|p29|||||||||
11284|Mareeba Granite|32665|6|Mentioned|p763|||||||||
11284|Mareeba Granite|33695|6|Mentioned|p3|||Plate 1. Permian. Refers Fardon & de Keyser (1964).||||||
11284|Mareeba Granite|34826|6|Mentioned|p29|||||||||
11284|Mareeba Granite|36353|6|Mentioned|p365|||||||||
11284|Mareeba Granite|36527|6|Mentioned|p164|||||||||
11284|Mareeba Granite|36563|6|Mentioned|Table 1|||||||||
11284|Mareeba Granite|37575|6|Mentioned|p178|||||||||
11284|Mareeba Granite|37633|6|Mentioned|Table 38|||||||||
11284|Mareeba Granite|39252|6|Mentioned|p22|||||||||
11284|Mareeba Granite|39445|5|Briefly described|Table 12|||||||||
11284|Mareeba Granite|39689|6|Mentioned|p56|||See also P58||||||
11284|Mareeba Granite|40049|6|Mentioned|Fig.2|||||||||
11284|Mareeba Granite|41235|6|Mentioned|p40|||||||||
11284|Mareeba Granite|42200|6|Mentioned|Fig.1 P325|||||||||
11284|Mareeba Granite|42304|5|Briefly described|p14|||||||||
11284|Mareeba Granite|42547|5|Briefly described|p75|||||||||
11284|Mareeba Granite|42625|5|Briefly described|Map legend|Late Permian|Carboniferous|||||||
11284|Mareeba Granite|42658|4|Described|p27, p33|||||||||
11284|Mareeba Granite|42810|3|Fully described|Table 1 P16|Late Permian|Early Permian|see also p22. Age: early Early Permian to early Late Permian||||||23-APR-09
11284|Mareeba Granite|43060|5|Briefly described|p105||Early Permian|of Whypalla Supersuite.||||||
11284|Mareeba Granite|43070|5|Briefly described|p92|||||||||
11284|Mareeba Granite|43098|6|Mentioned|p31|||||||||
11284|Mareeba Granite|43259|4|Described|Appendix 1,p37.||Permian|||||||
11284|Mareeba Granite|43625|5|Briefly described|p125,Appendix 6|||||||||
11284|Mareeba Granite|43896|14|Not recorded|Map Legend||Permian|||||||
11284|Mareeba Granite|43898|14|Not recorded|Map Legend||Carboniferous|||||||
11284|Mareeba Granite|43903|14|Not recorded|Map Legend||Early Permian|Early Permian to Middle (?) Carboniferous||||||
11284|Mareeba Granite|43927|14|Not recorded|p11,19,25,opp.8|||||||||
11284|Mareeba Granite|43979|14|Not recorded|p67,68|||||||||
11284|Mareeba Granite|44258|14|Not recorded|p1,5,11,12,15,18,33,||Permian|264+/-2 Ma. p34,39,40||||||
11284|Mareeba Granite|44259|14|Not recorded|p109|||264+/-2 Ma.||||||
11284|Mareeba Granite|44292|14|Not recorded|Tb.1,opp.p8|||Correlated with Altanmoui, Puckley and Finlayson Granite.||||||
11284|Mareeba Granite|44293|14|Not recorded|Map Legend||Permian|||||||
11284|Mareeba Granite|44294|2|Defined|Tb.2,p10,12,map|||||||||
11284|Mareeba Granite|44296|14|Not recorded|Map Legend||Carboniferous|||||||
11284|Mareeba Granite|44329|14|Not recorded|p4,6-7,10|||Once thought Late Carboniferous, now dates as Early Permian.||||||
11284|Mareeba Granite|44330|14|Not recorded|Map Legend||Early Permian|||||||
11284|Mareeba Granite|44425|14|Not recorded|p17-18,22,map|||||||||
11284|Mareeba Granite|44560|14|Not recorded|p359|||||||||
11284|Mareeba Granite|44589|14|Not recorded|p387|||||||||
11284|Mareeba Granite|44880|14|Not recorded|unknown (p195-208)|||||||||
11284|Mareeba Granite|45003|14|Not recorded|p30|||||||||
11284|Mareeba Granite|45014|14|Not recorded|p103-4,124-6,140|||||||||
11284|Mareeba Granite|45025|4|Described|p76-7,anal.p83-85||Permian|||||||
11284|Mareeba Granite|45065|6|Mentioned|p48|||||||||
11284|Mareeba Granite|45087|5|Briefly described|p10|||Chemical analyses||||||
11284|Mareeba Granite|45113|3|Fully described|p20|||Emphasis on petrography.||||||
11284|Mareeba Granite|45686|14|Not recorded|p.356|||Probably intrudes Hodgkinson Beds.||||||
11284|Mareeba Granite|46845|6|Mentioned|Table 1|||||||||
11284|Mareeba Granite|46879|6|Mentioned|Fig.1|||||||||
11284|Mareeba Granite|48764|6|Mentioned|p112|||||||||
11284|Mareeba Granite|48894|6|Mentioned|p56|||Age. See also PP57,59.||||||
11284|Mareeba Granite|48976|4|Described|p36|||Isotopic data Table 8||||||
11284|Mareeba Granite|50387|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Kennedy Province. Age: 282 +/- 9 Ma (Rb-Sr). Of Whypalla Supersuite||||||
11284|Mareeba Granite|50542|6|Mentioned|p96|Paleozoic|Paleozoic|||||||07-FEB-11
11284|Mareeba Granite|60425|4|Described|p35, p80, p274-5 Appdx. 1|Early Permian|Early Permian|Of Mareeba Suite (Whypalla S'suite). Originally extended to units now forming Bellenden Ker Batholith. Parts subsequently mapped as Mount Formartine Granite. Age: 278Ma, 279Ma (Rb-Sr). Muscovite-biotite granite, S-type - detailed lithology on p275.||||||07-FEB-11
11284|Mareeba Granite|66180|6|Mentioned|pp280-282|||||||||10-MAY-12
11284|Mareeba Granite|68576|5|Briefly described|Q_11: p6|||Mareeba area. Crops out as whalebacks. Part of the Kennedy Igneous Association.|||||Muscovite-biotite granite. S-type.|
11284|Mareeba Granite|69593|5|Briefly described|p479, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|280 Ma.|Mareeba Suite.|||S-type.|
11284|Mareeba Granite|72298|6|Mentioned|p792|||Part of the basement to Quaternary sediments hosting aquifers in the Barron Delta and Mulgrave River areas.||||||
11297|Maria Formation|13516|5|Briefly described|p145 fig 3|Late Permian|Late Permian|From Comet Ridge, Bowen Basin. Age: APP5002 - APP5003||||||
11297|Maria Formation|22978|6|Mentioned|p148 Fig.1|||||||||
11297|Maria Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
11297|Maria Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
11297|Maria Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: >259Ma.  Geological Province: Bowen Basin.||||||
11297|Maria Formation|31079|6|Mentioned|Fig. 6|||||||||
11297|Maria Formation|31531|6|Mentioned|p11|||U.Permian||||||
11297|Maria Formation|31656|4|Described|Table 1|||U.Permian. Blenheim Sub-Gp.||||||
11297|Maria Formation|31690|4|Described|p41|||Mention p35, name extended.||||||10-MAY-21
11297|Maria Formation|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
11297|Maria Formation|32577|4|Described|p23|Late Permian|Early Permian|See also p24,27-29. L.-U.Perm.||||||10-MAY-21
11297|Maria Formation|32689|1|Redefined|p436|Permian|Permian|||||||
11297|Maria Formation|33390|6|Mentioned|p3|||Refers Prouza & Park (1973)||||||
11297|Maria Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
11297|Maria Formation|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin||||||
11297|Maria Formation|36739|6|Mentioned|p24|||||||||
11297|Maria Formation|37070|6|Mentioned|p69|||||||||
11297|Maria Formation|37072|6|Mentioned|p91|||||||||
11297|Maria Formation|37076|5|Briefly described|p121|||||||||
11297|Maria Formation|37612|6|Mentioned|p283|||See also Fig.3||||||
11297|Maria Formation|37726|6|Mentioned|Fig.2|||||||||
11297|Maria Formation|38518|6|Mentioned|Fig.3|||||||||
11297|Maria Formation|38958|6|Mentioned|p493|||||||||
11297|Maria Formation|39261|6|Mentioned|Fig.6|||||||||
11297|Maria Formation|39267|6|Mentioned|p239|||||||||
11297|Maria Formation|39268|6|Mentioned|Fig.4|||||||||
11297|Maria Formation|39272|5|Briefly described|p295|||Correlation||||||
11297|Maria Formation|39273|6|Mentioned|Fig. 2|||||||||
11297|Maria Formation|39445|5|Briefly described|Table 8|||||||||
11297|Maria Formation|40321|6|Mentioned|p20|||See also Fig.4||||||
11297|Maria Formation|40675|6|Mentioned|Table 5A|||Mention Table 5C||||||
11297|Maria Formation|41191|6|Mentioned|Fig.3|||||||||
11297|Maria Formation|41246|6|Mentioned|Map legend|Permian||||||||
11297|Maria Formation|41809|6|Mentioned|p64|||||||||
11297|Maria Formation|42249|6|Mentioned|Table 1 P22|||||||||
11297|Maria Formation|42250|6|Mentioned|Fig.4 P31|||||||||
11297|Maria Formation|42251|6|Mentioned|Fig.2 P38|||||||||
11297|Maria Formation|42641|6|Mentioned|Fig.3 P110|||||||||
11297|Maria Formation|42662|6|Mentioned|p85|||||||||
11297|Maria Formation|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
11297|Maria Formation|43050|5|Briefly described|p15|||||||||
11297|Maria Formation|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|||||||
11297|Maria Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
11297|Maria Formation|44424|14|Not recorded|p293-301|||At base of Blenheim Subgroup.||||||
11297|Maria Formation|44514|2|Defined|p33,34||Artinskian|Conformably overlain by Crocker Formation. Plants and spores. (Late Artinskian)||||||
11297|Maria Formation|44571|2|Defined|p207|||May correlate with Catherine Sandstone.||||||
11297|Maria Formation|44618|4|Described|p511,513-4,516-8,520||Permian|Equated to lower silty part of Peawaddy Formation.||||||
11297|Maria Formation|45071|3|Fully described|Table 10|||||||||
11297|Maria Formation|48847|14|Not recorded|Pl.2|||||||||
11297|Maria Formation|48898|4|Described|p38|||See also PP27,34,35 etc. U.Permian||||||
11297|Maria Formation|48915|6|Mentioned|Table 3|||||||||
11297|Maria Formation|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
11297|Maria Formation|63773|6|Mentioned|p1059|||||||||
11297|Maria Formation|67402|6|Mentioned|p21, p45, p85 tbl BWN2|Capitanian|Capitanian|Bowen Basin.||||Overlain by the German Creek Formation. Overlies the Aldebaran Formation, Upper.||
11297|Maria Formation|68679|5|Briefly described|p378, p380-381|Permian|Permian|Prouza and Park (1973); Dickins and Malone (1973). Bowen Basin. 240m thick. Offshore marine sediments.||||Overlies Freitag Formation. Passes laterally into Ingelara Formation. Is overlain by German Creek Formation.|Mudstone, siltstone, sandstone, minor tuff; marine fossils.|
11297|Maria Formation|71276|5|Briefly described|p294|Permian|Permian|Prouza and Park (1973). Bowen Basin. In the Galilee Basin, this unit, with the Blenheim Formation, is known as the Ingelara Formation.||||||
11326|Marion Formation|31572|4|Described|Fig. 1|||Tertiary||||||
11326|Marion Formation|33073|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11326|Marion Formation|34454|5|Briefly described|Table 1|||Tertiary||||||
11326|Marion Formation|35121|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11326|Marion Formation|35139|4|Described|Table.2|||||||||
11326|Marion Formation|37607|4|Described|p333|||See also Fig.4||||||
11326|Marion Formation|38532|4|Described|Fig.4|||||||||
11326|Marion Formation|39445|5|Briefly described|Table 14|||||||||
11326|Marion Formation|42746|6|Mentioned|p18|||||||||
11326|Marion Formation|44066|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44088|14|Not recorded|Tb.1,opp.p6,8,map|||||||||
11326|Marion Formation|44119|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44120|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44121|14|Not recorded|p6-9,12|||||||||
11326|Marion Formation|44122|14|Not recorded|p322|||||||||
11326|Marion Formation|44133|5|Briefly described|p190 Fig. 10.30|Eocene|Paleocene|||||||
11326|Marion Formation|44168|4|Described|p6-8,map|||Correlated with Eyrian Series. Birdsville sheet.||||||
11326|Marion Formation|44291|2|Defined|Tb.1,p6,10,13,map|||||||||
11326|Marion Formation|44308|14|Not recorded|p11,12,Tb.2||Tertiary|||||||
11326|Marion Formation|44309|2|Defined|Tb.1,opp.p7,14,map||Tertiary|||||||
11326|Marion Formation|44310|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44312|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44313|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44326|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44351|2|Defined|p11,12,18,20-25,|||Pls.7,12. Conformably overlies Wilgunya Formation. Overlain by Noranside Limestone and Austral Downs Limestone.||||||
11326|Marion Formation|44361|14|Not recorded|Map Legend||Tertiary|||||||
11326|Marion Formation|44362|14|Not recorded|unknown|||||||||
11326|Marion Formation|44543|2|Defined|p35,36||Tertiary|Probably same as Eyrian Series.||||||
11326|Marion Formation|45052|4|Described|p136|||Cainozoic||||||
11326|Marion Formation|50100|6|Mentioned|p23|Cenozoic|Cenozoic|||||||
11326|Marion Formation|61155|5|Briefly described|p16|Middle Eocene|Late Paleocene|Age: ~60-40Ma. Thickness: 45m. Geological Province: Georgina Basin.||||||
11326|Marion Formation|63450|6|Mentioned|p83|Cenozoic|Cenozoic|Geological province: Georgina Basin.||||||07-FEB-11
11326|Marion Formation|64047|2|Defined|p60-61|Tertiary|Tertiary|Of Casey (1959). Overlain by Austral Downs Limestone. Min. thick: 8m. Comprises quartzose sandstone and quartz pebble conglomerate; chert clasts present and reworked laterised sandstone clasts at base.||||||
11326|Marion Formation|66131|5|Briefly described|p240, p242 Fig.2|Eocene|Paleocene|Late Paleocene to Late Eocene in age (from p.242 Fig.2 - stratigraphic correlation chart).||||Correlative of the Eyre Formation.||
11326|Marion Formation|66623|6|Mentioned|p273.|||Lateral equivalent of Eyre Formation.||||||
11326|Marion Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.||||Underlies and may interfinger with Noranside Limestone|Fluviatile and lacustrine quartzose sandstone, quartzose conglomerate, minor sandy siltstone; lateritised and silicified.|
11326|Marion Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
11326|Marion Formation|69599|5|Briefly described|p584, p599-600|Eocene|Paleocene|Marion Basin. Equivalent outcrops occur as far south as the SA border. Up to 45m thick. Fluviatile sediments. No biostratigraphically useful fossils. Capped by silcrete and laterite of the Canaway profile.||||Is locally overlain by Noranside Limestone. Correlated (at least partly) with Eyre, Glendower, Edkins, Springvale and Moonie Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.|Mostly silicified quartz sandstone and fine-grained quartz conglomerate with sporadic fossil wood.|
11331|Marlborough Metamorphics|22740|6|Mentioned|156 fig 2|||Geol. province: New England Fold Belt.||||||14-FEB-07
11331|Marlborough Metamorphics|24615|5|Briefly described|CD|Late Paleozoic|Late Paleozoic|[Pzm/m].  Muscovite-biotite gneiss and schist, micaceous quartzite, chlorite schist, phyllite, minor marble and diopside-labradorite hornfels and amphibolite.||||||07-NOV-08
11331|Marlborough Metamorphics|42868|5|Briefly described|Fig.2 P16|||||||||
11331|Marlborough Metamorphics|50209|5|Briefly described|Map Legend|Paleozoic|Paleozoic|||||||07-NOV-08
11331|Marlborough Metamorphics|60481|5|Briefly described|Map Legend|Early Paleozoic|Neoproterozoic|Includes: Nob Creek Amphibolite. Muscovite-biotite gneiss and schist, quartzite, orthogneiss and amphibolite.||||||07-NOV-08
11331|Marlborough Metamorphics|60557|5|Briefly described|p17, p18 Fig. 5ab|Carboniferous|Devonian|Include rocks that are very similar to units of the Curtis Island Group. See also p19 Fig. 5b.||||||28-MAY-08
11331|Marlborough Metamorphics|61035|5|Briefly described|p16, p17|||Includes; Nob Creek Amphibolite. Consists of gneiss and schists, quartzite, orthogneiss; minor marble and hornfels and amphibolite are present. Lower amphibolite facies rocks. Geological Province: Marlborough Block, Wandilla Province.||||||07-FEB-11
11331|Marlborough Metamorphics|65388|4|Described|p151-153; p152 Fig.61, p70, 150, 156|Permian|Late Devonian.|Marlborough Block.Name used by Morand (1993a, 1998) but "Windermere Metamorphics" by Harbort (2001). Includes Nob Creek Amphibolite. Imbricated thrust slices in contact with Princhester Serpentinite. Intruded by Cleethorpes Granodiorite, Og Syenite, Magog Gabbro. Cooling age (metamorphic age?) Permian to early Triassic. Deposition likely to be Late Devonian. Correlated with Broome Head Metamorphics.  Area of ~300km2. No type locality designated. Phyllite, pelitic schist, feldspathic schist and amphibolite. Probably originally a succession of quartzose sandstone, mudstone, mafic lavas and possibly chert intruded by granite.||||||
11331|Marlborough Metamorphics|68008|3|Fully described|p7-8, p174, p303, p306-307, p484|||In the Marlborough Block, forms NW-trending belts of alternating slices with Princhester Serpentinite: structure and timing detailed. Subdued topography: low rounded hills. A thin-skinned nappe sheet (<2km thick). Over 6km thick (thickened by folding). Age of metamorphism ~245 Ma; age of protolith unknown. Underlay the Canoona goldfield (source of the gold was probably adjacent serpentinite). Other similar ages given.|c.248-242 Ma.|||Faulted against Princhester Serpentinite.|Central and eastern parts are metasediments: pyllite, chlorite schist, local muscovite or amphibole-bearing schist. Western belt, now a biotite schist, was originally a foliated granite. Lower amphibolite facies S-type granite, and metabasite.|
11331|Marlborough Metamorphics|68553|6|Mentioned|Map legend|Early Paleozoic|Neoproterozoic|||||||
11331|Marlborough Metamorphics|68679|5|Briefly described|p308-309, p312-313, p347, p426|Late Devonian|Late Devonian|Morand et al. (1993, 1998). Marlborough Block. Metasedimentary rocks and S-type metagranite. Crops out over ~300 km2 in sinuous NW-trending belts, from Glen Geddes to Marlborough.|||Nob Creek Amphibolite.|Imbricated with Princhester Serpentinite. Is intruded by Cleethorpes Granodiorite, Og Syenite and Magog Gabbro.|Phyllite, pelitic schist (hosting subeconomic mineralisation) and feldspathic schist (may have had a granitic protolith).|
11331|Marlborough Metamorphics|69952|6|Mentioned|p75|Paleozoic|Neoproterozoic|||||||23-NOV-15
11343|Maronghi Creek beds|23440|5|Briefly described|p139|Permian|Carboniferous|||||||
11343|Maronghi Creek beds|23799|3|Fully described|p8, p14 Tb. 1|Carboniferous|Devonian|Formerly referred to as Neranleigh-Ferndale beds equivalents.  Formerly included the "Wondai Series" (Reid, 1925).  Geological Province: Yarraman Subprovince (Wandilla Province). See also p65 Fig. 5.||||||
11343|Maronghi Creek beds|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
11343|Maronghi Creek beds|24560|5|Briefly described|Map legend|Carboniferous|Devonian|Mudstone, shale, arenite, chert, jasper, acid to basic metavolcanics.||||||
11343|Maronghi Creek beds|40475|5|Briefly described|p3|||||||||
11343|Maronghi Creek beds|40485|6|Mentioned|p74|||||||||
11343|Maronghi Creek beds|40486|6|Mentioned|p83|||||||||
11343|Maronghi Creek beds|40488|6|Mentioned|p92|||||||||
11343|Maronghi Creek beds|41917|6|Mentioned|Fig.3 P528|||||||||
11343|Maronghi Creek beds|43008|5|Briefly described|map legend|||||||||
11343|Maronghi Creek beds|44923|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
11343|Maronghi Creek beds|50320|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman subprovince (Wandilla Province).||||||09-JUN-04
11343|Maronghi Creek beds|50384|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince.||||||
11343|Maronghi Creek beds|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince. Mudstone, shale, arenite, chert, jasper, acid to basic metavolcanics.||||||02-SEP-04
11343|Maronghi Creek beds|60371|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince. Mudstone, shale, arenite, chert, jasper, acid to basic metavolcanics.||||||
11343|Maronghi Creek beds|60993|5|Briefly described|p17, p6 Fig. 2|Paleozoic|Paleozoic|Unconformably overlain by Marburg Subgroup units.||||||07-NOV-08
11343|Maronghi Creek beds|61781|4|Described|p267|Early Mesozoic|Early Carboniferous|Divided into 5 elements.||||||
11343|Maronghi Creek beds|63821|6|Mentioned|p19|||Geological Province: Yarraman Block.||||||07-FEB-11
11343|Maronghi Creek beds|65003|4|Described|p1,p5, p26|Early Carboniferous|Late Devonian|?Late Devonian to Early Carboniferous. Of Wandilla Province. Highly structurally deformed metasediments.||||Intruded by the Permo-Triassic Boondooma Igneous Complex and the Triassic granitoids of the Toondahra Granite.|Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid-bearing sandstone, conglomerate with mudstone rip-up clasts, and oolitic and pisolitic limestone.|30-MAR-12
11343|Maronghi Creek beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Yarraman Subprovince. This unit, as well as Bjelke Petersen beds, Fifer Creek, Sugarloaf and Mountefontein Metamorphics, and unnamed sedimentary units, are all mapped under the symbol, DCym.||||||
11343|Maronghi Creek beds|68679|5|Briefly described|p321-324, p397 Fig.5.77, p413|Carboniferous|Devonian|Cranfield and Schwarzbock (1973). Northern New England Orogen. The most extensive unit in the Yarraman Subprovince, Wandilla Province. Forms a 25km wide, NNW-trending belt. Accretionary rocks. Unfossiliferous. Age range based on similar accretionary wedges in the Orogen. Intruded by early Permian (296 Ma, 291 Ma) microdiorite. Forms E margin of Tarong Basin. Is intruded by Boondooma Igneous Complex.||||Is overlain unconformably by Gilla Volcanics, Neara Volcanics, Tarong beds, Main Range Volcanics. Is faulted against Sugarloaf Metamorphics, Bjelke-Petersen beds and ? Esk Formation.|Interbedded massive to poorly sorted quartz lithic to lithic sandstone, siltstone and mudstone with weathered spilitic volcanics and rare schist and amphibolite. Locally abundant quartz veining; local melange.|
11343|Maronghi Creek beds|69582|5|Briefly described|p82, p84, p86|Carboniferous|Devonian|Yarraman Subprovince, Wandilla Province. Beds strike north-south and dip steeply to east and west. This unit outcrops extensively to the east of the Tarong Basin.||||Intruded by the Boondooma Igneous Complex. Unconformably overlain by the Tarong beds.|Fine-grained sedimentary sequences and mafic sea floor lavas.|
11345|Maroondan Basalt|42895|3|Fully described|p69|||probable early Pliocene age. Variation on Maroondan Melanephelinite?||||||
11345|Maroondan Basalt|68332|5|Briefly described|Map legend.|Neogene|Neogene|Bundaberg Volcanic Province.|||||Fine-grained, grey-black hawaiite-basalt.|
11345|Maroondan Basalt|68421|5|Briefly described|Map Legend|Pliocene|Miocene|Bundaberg Volcanic Province.|||||Fine-grained, grey-black hawaiite-basalt.|
11361|Marraba Volcanics|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Malbon Group. Includes: Timberoo Member, Cone Creek Metabasalt Member. Underlies: Mitakoodi Quartzite. Overlies: Argylla Formation.||||||27-AUG-04
11361|Marraba Volcanics|22461|5|Briefly described|Fig 1 p464|||Of the Malbon Group.||||||02-NOV-06
11361|Marraba Volcanics|22498|6|Mentioned|Fig1 P234|||||||||
11361|Marraba Volcanics|22747|6|Mentioned|Table1,p7|||Correlates in part with Eastern Creek Volcanics||||||
11361|Marraba Volcanics|23071|5|Briefly described|p760|Statherian|Statherian|||||||
11361|Marraba Volcanics|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1755-1760Ma.||||||02-NOV-06
11361|Marraba Volcanics|23519|5|Briefly described|p110 Table 1|Mesoproterozoic|Mesoproterozoic|||||||
11361|Marraba Volcanics|24253|5|Briefly described|p4|||Geological Province: Mitakoodi Block, Mount Isa Block.||||||
11361|Marraba Volcanics|24254|5|Briefly described|p21|Proterozoic|Proterozoic|Age: ca. 1760-1755 Ma (SHRIMP U-Pb). Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
11361|Marraba Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Mafic. Geological Province: Eastern Fold Belt.||||||
11361|Marraba Volcanics|29969|5|Briefly described|p393|||||||||
11361|Marraba Volcanics|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11361|Marraba Volcanics|30530|1|Redefined|p515|Precambrian|Precambrian|Also mentioned p515.||||||02-NOV-06
11361|Marraba Volcanics|30536|6|Mentioned|p100|||Stratigraphy||||||
11361|Marraba Volcanics|31704|6|Mentioned|p4|||Copper mineralization||||||
11361|Marraba Volcanics|32660|5|Briefly described|Table 5|||||||||
11361|Marraba Volcanics|32959|6|Mentioned|Fig.21|||||||||
11361|Marraba Volcanics|33214|6|Mentioned|Fig.1|||||||||
11361|Marraba Volcanics|33561|6|Mentioned|p102|||||||||
11361|Marraba Volcanics|33900|5|Briefly described|p16|||Mention p15.||||||02-NOV-06
11361|Marraba Volcanics|35074|6|Mentioned|Fig.2|||||||||
11361|Marraba Volcanics|35121|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11361|Marraba Volcanics|35139|4|Described|Table.2|||||||||
11361|Marraba Volcanics|35286|6|Mentioned|Fig.17|||||||||
11361|Marraba Volcanics|35295|6|Mentioned|p602|||||||||
11361|Marraba Volcanics|37568|5|Briefly described|p81|||||||||
11361|Marraba Volcanics|37569|6|Mentioned|p92|||||||||
11361|Marraba Volcanics|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11361|Marraba Volcanics|37862|6|Mentioned|p587|||||||||
11361|Marraba Volcanics|38234|4|Described|p104|||||||||
11361|Marraba Volcanics|38276|6|Mentioned|Fig.1|||||||||
11361|Marraba Volcanics|38350|4|Described|p10|||||||||
11361|Marraba Volcanics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11361|Marraba Volcanics|38834|6|Mentioned|p162|||||||||
11361|Marraba Volcanics|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
11361|Marraba Volcanics|39202|6|Mentioned|Fig.3|||||||||
11361|Marraba Volcanics|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11361|Marraba Volcanics|39445|6|Mentioned|p42|||See also Table 2||||||
11361|Marraba Volcanics|39496|4|Described|p5|||||||||
11361|Marraba Volcanics|39622|6|Mentioned|p19|||See also p29.||||||02-NOV-06
11361|Marraba Volcanics|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
11361|Marraba Volcanics|39924|6|Mentioned|p349|||||||||
11361|Marraba Volcanics|40840|6|Mentioned|Map legend|||||||||
11361|Marraba Volcanics|41306|4|Described|p5|||||||||
11361|Marraba Volcanics|41761|6|Mentioned|p284|||||||||
11361|Marraba Volcanics|41791|6|Mentioned|p248|||||||||
11361|Marraba Volcanics|41978|6|Mentioned|p501|||||||||
11361|Marraba Volcanics|41979|6|Mentioned|p536|||||||||
11361|Marraba Volcanics|42166|5|Briefly described|p108|||||||||
11361|Marraba Volcanics|42565|5|Briefly described|Table 1 P5, P3|||||||||
11361|Marraba Volcanics|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Malbon Group. Mafic volcanics, siltstone, sandstone.||||||09-FEB-09
11361|Marraba Volcanics|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
11361|Marraba Volcanics|44271|2|Defined|p28,29,33,42,50-1||Paleoproterozoic|||||||07-NOV-08
11361|Marraba Volcanics|44275|14|Not recorded|Map Legend|||||||||
11361|Marraba Volcanics|44276|2|Defined|p11,17,Tb.1,map|||||||||
11361|Marraba Volcanics|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
11361|Marraba Volcanics|44278|2|Defined|p5,7,Tb.1,map|||||||||
11361|Marraba Volcanics|44279|14|Not recorded|Tb.1|||||||||
11361|Marraba Volcanics|44521|14|Not recorded|p3,8|||||||||
11361|Marraba Volcanics|44765|14|Not recorded|p14-16||Paleoproterozoic|||||||07-NOV-08
11361|Marraba Volcanics|44806|14|Not recorded|p287|||||||||
11361|Marraba Volcanics|44920|14|Not recorded|Map Legend,Sheet 4||Carpentarian|||||||
11361|Marraba Volcanics|44989|2|Defined|p.71-3|||Tb.III. On many pages. Conformably overlies Argylla Formation; conformably underlies Mitakoodi Quartzite; Contemp.with Eastern Creek Volcanics and lavas of Soldiers Cap Formation. (F54-2,6).||||||02-APR-07
11361|Marraba Volcanics|45052|4|Described|p73|||||||||
11361|Marraba Volcanics|45136|6|Mentioned|p24|||||||||
11361|Marraba Volcanics|45161|4|Described|p40|||||||||
11361|Marraba Volcanics|45166|5|Briefly described|p20|||||||||
11361|Marraba Volcanics|45287|14|Not recorded|p.225,226|||||||||
11361|Marraba Volcanics|46801|6|Mentioned|p126|||See also Fig. 14||||||
11361|Marraba Volcanics|46960|6|Mentioned|p220|||||||||
11361|Marraba Volcanics|46962|4|Described|Table 1|||See also Fig.3.||||||
11361|Marraba Volcanics|49041|6|Mentioned|Table 4|||||||||
11361|Marraba Volcanics|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Includes the Cone Creek Metabasalt and Timberoo Members.  Predominantly basaltic lavas, with some calcareous and non-calcareous sitlstone and sandstone in upper levels.  Conformably overlie the Argylla Formation.  Geological Province: Eastern Fold belt.||||||20-JAN-05
11361|Marraba Volcanics|50125|6|Mentioned|p100|||Geological Province: Mount Isa Inlier||||||
11361|Marraba Volcanics|50332|6|Mentioned|p16|Paleoproterozoic|Paleoproterozoic|Age: 1800-1755Ma.||||||07-FEB-11
11361|Marraba Volcanics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Malbon Group. Metabasalt, metasiltstone, meta-arenite.||||||
11361|Marraba Volcanics|61922|5|Briefly described|p8, p9 Fig. 3, p15-16 Figs. 7 and 8|||Composed of two members - an upper mafic pelitic member and a lower basalt member. Overlies Argylla Formation unconformably in the Malbon Zone.  Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
11361|Marraba Volcanics|61924|5|Briefly described|p44|||Mafic-dominated unit. Geological Province: Eastern Fold Belt.||||||
11361|Marraba Volcanics|61925|5|Briefly described|p56 Fig. 1, p57 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of Malbon Gp.Mafic volcs. and fine clastic successions: lower thick succession of pink quartzo-feldspathic arenite, minor quartzite interbeds. Upper part unconform.over lower part. Conformable on Argylla Fm.Max.thick: 2300m.Geol.Prov: Leichardt Superbasin||||||07-NOV-08
11361|Marraba Volcanics|61926|5|Briefly described|p70-71|Paleoproterozoic|Paleoproterozoic|Of the Malbon Group. Metabasalt, mafic schist, foliated dolerite dykes. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||07-NOV-08
11361|Marraba Volcanics|61929|5|Briefly described|p127, p128 Fig. 2|||Of the Mary Kathleen Group. Geological Province: Leichhardt Superbasin.||||||
11361|Marraba Volcanics|61933|6|Mentioned|p176|||Overlain by Mitakoodi Quartzite.||||||
11361|Marraba Volcanics|61936|5|Briefly described|p190 Fig. 3|||Interbedded mafic volcanics and fine-grained clastic rocks. Overlain by Mitakoodi Quartzite. Geological Province: Eastern Fold Belt, Mount Isa Inlier. See also p195 Fig. 6.||||||
11361|Marraba Volcanics|63866|5|Briefly described|p62, p65|||Mitakoodi Anticline.|||Includes the Cone Creek Metabasalt Member, Mount Start Member and the Timberoo Member.|Overlain by the Mitakoodi Quartzite.||
11361|Marraba Volcanics|64248|5|Briefly described|p32, p33 Fig.1, p38 Fig.5, p40 Fig.6 |Statherian|Statherian|See also p41 Tb. 2, p43 Fig.11. Age range from under- and overlying units.|Between 1761 +/- 4 Ma and 1756 +/- 3 Ma.|||Overlies Argylla Formation. Is overlain by Mitakoodi Quartzite.||
11361|Marraba Volcanics|64250|5|Briefly described|Figs.2-5; p15, p19, p21-22|||Cloncurry Fold Belt, Mount Isa Inlier.||||Overlies Argylla Formation/Tewinga Group. Is overlain by Mitakoodi Quartzite.|Mafic lava (pillows near base); minor calcareous sandstone and siltstone (upper parts).|
11361|Marraba Volcanics|64251|6|Mentioned|p51 Fig. 1|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
11361|Marraba Volcanics|65396|5|Briefly described|p4, p7, p13-14, p16-17, p23, p77, p82|Statherian|Statherian|See also p84, p173, p175, p179, p182-183, p187, p190, p192-194, p199, p213, p222, p234-241, p267, p272, p439. Leichhardt Superbasin. Eastern Succession. Cover Sequence 2.|1760-1750 Ma|Malbon Group||Overlies Argylla Formation; overlain by Mitakoodi Quartzite.|Mafic volcanics (flood basalts).|
11361|Marraba Volcanics|65755|6|Mentioned|p3 Fig.1|||||||||
11361|Marraba Volcanics|66913|5|Briefly described|p170 fig 1, p172||||1700-1725 Ma|||Overlies Argylla Formation. Overlain by Mitakoodi Quartzite.|Mafic volcanic rocks and fine-grained siliciclastics.|
11361|Marraba Volcanics|67323|4|Described|GIS attrib tbl, p16, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mitakoodi Domain, Leichhardt Superbasin. Previously equated with the Eastern Creek Volcanics, but the latter are too old.|~1760 Ma.|Malbon Group|Timberoo, Mount Start Members.|Overlies Bulonga Volcanics. Is overlain by Mitakoodi Quartzite.|Mainly metabasalt (flows), with amphibolite, meta-arenite, schist; minor chert.|
11361|Marraba Volcanics|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Eastern Succession. Shown as including hiatus and being partly equivalent to Myally Supersequence and partly to Quilalar Supersequence.||||Overlain by Mitakoodi Quartzite, intruded by Wonga Granite, Burstal Granite. Inferred correlation with Eastern Creek Volcanics. Lower part equivalent to Argylla Formation.|Basaltic lava flows with some interbeds of shallow marine, stromatolitic dolostone near base.|
11361|Marraba Volcanics|68146|5|Briefly described|p78|||Mitakoodi Block. May be equivalent in age to the c.1752 Ma Double Crossing Metamorphics in the adjacent Eastern Fold Belt.|||Timberoo Member.||Includes fine-grained metasedimentary rocks and mafic volcanics.|
11361|Marraba Volcanics|68542|6|Mentioned|p16 fig 4|||||||||
11361|Marraba Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with Mitakoodi Quartzite under the symbol, -Pn.||||||
11361|Marraba Volcanics|68575|5|Briefly described|p2, p47, p126|||Mitakoodi Domain. May be age-equivalent to Double Crossing Metamorphics.|||Timberoo Member.||Includes fine-grained metasedimentary rocks as well as mafic volcanics.|
11361|Marraba Volcanics|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 2 (1725-1700 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
11361|Marraba Volcanics|69056|5|Briefly described|p52-53, Time-Space plot sheet|Statherian|Statherian|Eruption of these rocks marked the end of Bulonga Volcanics volcanism in the Duck Creek area. Previously equated with the Eastern Creek Volcanics (in westen part of Mount Isa Inlier) but are much younger.|||Timberoo Member.|Overlies Bulonga Volcanics. Is overlain by Mitakoodi Quartzite.|Mafic volcanics.|
11361|Marraba Volcanics|69222|6|Mentioned|p222 Fig.2, p223|Statherian|Statherian|Eastern Fold Belt. Associated with the Myally Rift Event.||||Overlain by Mitakoodi Quartzite||09-FEB-18
11361|Marraba Volcanics|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Metabasalt, amphibolite, metasandstone and schist; minor chert|
11361|Marraba Volcanics|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|||Malbon Group|||Metabasalt, amphibolite, metasandstone and schist; minor chert|
11361|Marraba Volcanics|69591|4|Described|p29, p33, p35, p50 Fig.2.42, p57, p105|Paleoproterozoic|Paleoproterozoic|Mitakoodi Domain, Leichhardt Superbasin, Mount Isa Province. Part of Myally Supersequence. Erupted rapidly (closely-spaced ages of surrounding units) in a subaqueous to shallow-marine environment. May correlate with Double Crossing Metamorphics.||Malbon Group.||Overlies Bulonga Volcanics. Is overlain by Mitakoodi Quartzite.|Tholeiitic basalt, passing upwards into predominantly argillaceous sedimentary rocks and some sandstone. Also described as: metabasalt, amphibolite, meta-arenite, schist; minor chert.|
11361|Marraba Volcanics|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Malbon Group.|Cone Creek Metabasalt, Mount Start, Timberoo, Members.|Is overlain by Mitakoodi Quartzite.||
11361|Marraba Volcanics|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Malbon Group.|Cone Creek Metabasalt, Mount Start, Timberoo, Members.|Is overlain by Mitakoodi Quartzite.||
11361|Marraba Volcanics|71799|4|Described|p150 fig 2, p151 fig 3, p154|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block. 700m thick.|ca. 1760 Ma||Includes the Timberoo and Mount Start members.|Overlies the Bulonga Volcanics. Overlain by the Mitakoodi Quartzite.|Basalt, pillow lavas interstratified with fine-grained sandstone or dolostone containing stromatolites and silica pseudomorphs after gypsum.|03-OCT-18
11361|Marraba Volcanics|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Malbon Group|Includes Timberoo Member, Mount Start Member, Cone Creek Metabasalt Member.||Metabasalt, amphibolite, meta-arenite and schist; minor chert.|30-JUL-20
11361|Marraba Volcanics|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Malbon Group|Includes Timberoo Member, Mount Start Member, Cone Creek Metabasalt Member.|||
11361|Marraba Volcanics|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as significantly older than the the Wonga-Burstall Event (c. 1740 Ma).||Malbon Group|Includes Timberoo Member, Cone Creek Metabasalt Member|Underlies Mitakoodi Quartzite. Bulonga Volcanics shown as underlying.|Metabasalt, amphibolite, metasandstone and schist; minor chert. Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
11361|Marraba Volcanics|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as significantly older than the the Wonga-Burstall Event (c. 1740 Ma).||Malbon Group|Includes Timberoo Member, Cone Creek Metabasalt Member|Underlies Mitakoodi Quartzite. Bulonga Volcanics shown as underlying.|Metabasalt, amphibolite, metasandstone and schist; minor chert. Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
11361|Marraba Volcanics|72889|6|Mentioned|p6 Fig.i.|||||||||
11361|Marraba Volcanics|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
11361|Marraba Volcanics|73525|6|Mentioned|p4-5 Fig.2|||Mitakoodi-Tommy Creek Domain.|||||Mafic extrusives, minor siliciclastics.|
11380|Marshs Creek Formation|23422|5|Briefly described|p183|Early Permian|Late Carboniferous|Of Sybil Group.||||||
11380|Marshs Creek Formation|23424|5|Briefly described|p339|Early Permian|Late Carboniferous|Similar age to Wade beds. Sybil Graben Province.||||||
11380|Marshs Creek Formation|23430|4|Described|p520|||||||||
11380|Marshs Creek Formation|23893|5|Briefly described|p19|Early Permian|Late Carboniferous|Of Sybil Group.||||||
11380|Marshs Creek Formation|24577|5|Briefly described|p754 Fig. 2|Late Paleozoic|Late Paleozoic|Overlies the Hell's Gate Rhyolite. Formation is Fmn in text. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||07-NOV-08
11380|Marshs Creek Formation|42547|4|Described|p76|||Variation on Marshs Creek beds.||||||
11380|Marshs Creek Formation|42690|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
11380|Marshs Creek Formation|42692|5|Briefly described|map legend|Permian|Late Carboniferous|||||||
11380|Marshs Creek Formation|43095|2|Defined|p71|Early Permian|Late Carboniferous|of Sybil Group. Redefinition of Marshs Creek Beds.||||||25-MAY-04
11380|Marshs Creek Formation|68350|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Sybil Group.|Includes Engow Member.|Conformably overlies Malairo Rhyolite Member (Hells Gate Rhyolite).|Lithofeldspathic sandstone, conglomerate, tuff, tuffaceous sandstone, siltstone and mudstone.|
11380|Marshs Creek Formation|68351|5|Briefly described|Map legend.|Early Permian|Late Carboniferous|Kennedy Province. Unit in Sybil Graben.||Unit in Sybil Group.|Includes Engow Member.|Conformably overlies Malairo Rhyolite Member (Hells Gate Rhyolite).|Lithofeldspathic sandstone, conglomerate, tuff, tuffaceous sandstone, siltstone and mudstone.|
11380|Marshs Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Balfes Creek, Ellenvale and Wade beds; Insolvency Gully Formation; and Silver Valley Conglomerate, are all mapped under the symbol, CPs.||||||
11380|Marshs Creek Formation|69592|5|Briefly described|p274 Fig.4.65, p275-276|Permian|Pennsylvanian|Sybil Graben. Up to 750m thick. Lacustrine to alluvial fan deposits. Age range from plant macrofossils and palynomorphs respectively.||Sybil Group.|Engow Member.||Fine-grained volcaniclastic sandstone, mudstone, chert and minor polymict conglomerate; overlain by conglomerate with abundant rhyolite clasts, interbedded with sandstone, siltstone and mudstone; upper part is sandstone, siltstone and mudstone.|
11387|Martins Well Limestone Member|22520|6|Mentioned|p18|||||||||
11387|Martins Well Limestone Member|23032|5|Briefly described|p25 fig6||Early Devonian|||||||
11387|Martins Well Limestone Member|23424|5|Briefly described|Table 8.1 p334.|Pragian|Lochkovian|Graveyard Creek Subprovince.||||||
11387|Martins Well Limestone Member|31502|5|Briefly described|p94|||See also P95 for age.||||||
11387|Martins Well Limestone Member|31977|6|Mentioned|p86|||Emsian & ?Couvinian||||||
11387|Martins Well Limestone Member|32624|6|Mentioned|p722|||Coral species||||||
11387|Martins Well Limestone Member|33326|6|Mentioned|p436|||Fauna.||||||
11387|Martins Well Limestone Member|33329|6|Mentioned|p119|||Emsian. Corals.||||||
11387|Martins Well Limestone Member|33392|6|Mentioned|p86|||see also P94. L.Dev. Fauna||||||
11387|Martins Well Limestone Member|33434|6|Mentioned|p3|||||||||
11387|Martins Well Limestone Member|33437|6|Mentioned|p65|||See also P66. Emsian. Refers Jell (1968)||||||
11387|Martins Well Limestone Member|34251|2|Defined|p6|Early Devonian|Early Devonian|Emsian ?||||||
11387|Martins Well Limestone Member|37573|4|Described|p202|||||||||
11387|Martins Well Limestone Member|37575|5|Briefly described|p183|||||||||
11387|Martins Well Limestone Member|41260|6|Mentioned|p107|||||||||
11387|Martins Well Limestone Member|41679|1|Redefined|p253|Pragian|Lochkovian|||||||
11387|Martins Well Limestone Member|41719|6|Mentioned|Fig.2|||||||||
11387|Martins Well Limestone Member|41739|6|Mentioned|Fig.2|||||||||
11387|Martins Well Limestone Member|42031|5|Briefly described|p760|||||||||
11387|Martins Well Limestone Member|42032|5|Briefly described|p495|||||||||
11387|Martins Well Limestone Member|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
11387|Martins Well Limestone Member|42933|3|Fully described|p74|||of Shield Creek Formation||||||
11387|Martins Well Limestone Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Shield Creek Formation.||||||
11387|Martins Well Limestone Member|44062|2|Defined|p6,7||Emsian|Basal Limestone unit of Broken River Formation.||||||
11387|Martins Well Limestone Member|50088|6|Mentioned|p469|||Of the Shield Creek Formation.||||||
11387|Martins Well Limestone Member|65214|6|Mentioned|p275|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
11387|Martins Well Limestone Member|66498|6|Mentioned|p43|Early Devonian|Early Devonian|||Shield Creek Formation.||||
11387|Martins Well Limestone Member|68336|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Shield Creek Formation.|||Bioclastic calcarenite (richly fossiliferous) with mudstone and sandstone.|
11387|Martins Well Limestone Member|68341|5|Briefly described|Map legend.|Early Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Shield Creek Formation.|||Bioclastic calcarenite (richly fossiliferous) with mudstone and sandstone.|
11387|Martins Well Limestone Member|69030|5|Briefly described|p6|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province).||Shield Creek Formation.||||
11387|Martins Well Limestone Member|69592|5|Briefly described|p260, p263-264|Pragian|Lochkovian|Graveyard Creek Subprovince, Broken River Province. 160m thick. Forms only discontinuous lenses to the north.||Shield Creek Formation.|||Bioclastic calcarenite, with widely fossiliferous packstone and wackestone, algal bioclasts and bioherms, and uncommon shale interbeds; over these are muddy calcarenite with common calcareous mudstone interbeds, with a diverse fauna including fish.|
11399|Marumba beds|22845|4|Described|p39,46,67-71,4,9|Permian|Carboniferous|After McLeod 1954.||||||
11399|Marumba beds|22846|6|Mentioned|p20,23,4,36,41,7,67||Permian|Part of the Capsize Creek Complex.||||||
11399|Marumba beds|23251|6|Mentioned|p3, Fig 2(c)|||Was previously included in the Gympie Group by Day & others (1978). Gympie Group.||||||
11399|Marumba beds|23440|5|Briefly described|p146|Early Permian|Early Permian|||||||
11399|Marumba beds|23799|5|Briefly described|p42, p125|Permian|Early Permian|Basal trough sediments.  Overlie Jimna Phyllite.  Geological Province:  North D'Aguilar Province.||||||
11399|Marumba beds|29963|5|Briefly described|p3|||Permian.||||||
11399|Marumba beds|39252|5|Briefly described|p22|||||||||
11399|Marumba beds|39943|6|Mentioned|Table 12A|||||||||
11399|Marumba beds|41917|6|Mentioned|p521|||||||||
11399|Marumba beds|43006|5|Briefly described|p240|||||||||
11399|Marumba beds|43588|6|Mentioned|p30||Late Devonian|||||||
11399|Marumba beds|44923|5|Briefly described|Map Legend||Permian|||||||
11399|Marumba beds|44925|5|Briefly described|Map Legend||Permian|||||||
11399|Marumba beds|50320|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Marumba Subprovince (Wandilla Province)||||||
11399|Marumba beds|60370|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Gympie Province (Marumba Subprovince). Mudstone, sandstone, conglomerate, rhyolite.||||||02-SEP-04
11399|Marumba beds|63821|5|Briefly described|p19|Early Permian|Early Permian|Geological Province: Esk Trough.||||||07-FEB-11
11399|Marumba beds|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with the Northbrook and Cambroon beds; the Cedarton Volcanics, and the Kandanga Creek Megabreccia, are all mapped under the symbol, Pn.||||||
11399|Marumba beds|68679|5|Briefly described|p321, p324-326, p330-331, p369, p384-387|Permian|Permian|See also p389, p411. Brooks (1971); Sliwa (1994), and others (listed). Cressbrook Basin, northern New England Orogen; previously included in the Esk Basin. Cover basin sediments; some detritus derived from underlying basement granodiorite. Moderately dipping; low-grade metamorphosed with incipient cleavage. Contains marine fossils. Subaqueous debris flows or turbidites; ~1500m thick. Probably correlates with Cambroon beds, Kandanga Creek Megabreccia and Cedarton Volcanics. Is faulted against and unconformably overlain by Toogoolawah Group.||||Is faulted against/over or unconformably overlies Jimna Phyllite, Amamoor beds and Gallangowan Granodiorite. Underlies Bryden Formation. Intruded by Avoca Creek, Kimbala, Kingaham Creek Granodiorites.|Volcaniclastic sediments: thick monotonous lithic sandstone with lesser siltstone, or polymict conglomerate with thinly-bedded siltstone and sandstone; minor rhyolitic flows and an andesite flow.|
11409|Maryborough Formation|9194|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Mudstone, shale, siltstone, sandstone, and greywacke. Overlies Graham's Creek Formation; overlain by Burrum Coal Measures.||||||14-AUG-08
11409|Maryborough Formation|23251|6|Mentioned|p24||Cretaceous|Nambour Basin or Maryborough??||||||
11409|Maryborough Formation|23841|4|Described|p448|Early Cretaceous|Early Cretaceous|Geological Province: Maryborough Basin.  Maximum thickness: 2447m.||||||
11409|Maryborough Formation|24382|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||||||
11409|Maryborough Formation|29651|3|Fully described|p5|||See table 1 & Fig.5||||||
11409|Maryborough Formation|30446|6|Mentioned|p38|||||||||
11409|Maryborough Formation|30654|4|Described|p50|||See also P51,54-56. Aptian age||||||
11409|Maryborough Formation|30655|3|Fully described|p23|||See also Table 1||||||
11409|Maryborough Formation|30771|4|Described|p1|||||||||
11409|Maryborough Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
11409|Maryborough Formation|31086|6|Mentioned|p37|||Faunas||||||
11409|Maryborough Formation|32137|6|Mentioned|p355|||||||||
11409|Maryborough Formation|32774|5|Briefly described|Table 2|||||||||
11409|Maryborough Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
11409|Maryborough Formation|34287|6|Mentioned|p183|||||||||
11409|Maryborough Formation|35053|5|Briefly described|p37|||||||||
11409|Maryborough Formation|35688|6|Mentioned|Fig.2|||||||||
11409|Maryborough Formation|35813|6|Mentioned|p575|||||||||
11409|Maryborough Formation|35937|6|Mentioned|Fig.5|||||||||
11409|Maryborough Formation|36101|6|Mentioned|p171|||||||||
11409|Maryborough Formation|36243|6|Mentioned|Table 9A|||||||||
11409|Maryborough Formation|36574|4|Described|p599|||Palynostratigraphy.||||||
11409|Maryborough Formation|36575|4|Described|p597|||||||||
11409|Maryborough Formation|36581|6|Mentioned|Fig.1|||||||||
11409|Maryborough Formation|36772|6|Mentioned|p131|||See also P133, 134, 135||||||
11409|Maryborough Formation|36926|6|Mentioned|p165|||||||||
11409|Maryborough Formation|37118|6|Mentioned|Fig.1|||||||||
11409|Maryborough Formation|37120|6|Mentioned|p321|||||||||
11409|Maryborough Formation|37618|6|Mentioned|p15|||||||||
11409|Maryborough Formation|37861|6|Mentioned|p591|||||||||
11409|Maryborough Formation|38309|6|Mentioned|p227|||||||||
11409|Maryborough Formation|38391|6|Mentioned|p11|||||||||
11409|Maryborough Formation|38397|4|Described|Table 2|||||||||
11409|Maryborough Formation|38402|6|Mentioned|p72|||||||||
11409|Maryborough Formation|39211|5|Briefly described|p41|||Aptian. See Fig. 25||||||
11409|Maryborough Formation|39315|6|Mentioned|Fig.5|||||||||
11409|Maryborough Formation|39445|5|Briefly described|Table 11|||||||||
11409|Maryborough Formation|39505|6|Mentioned|p175|||||||||
11409|Maryborough Formation|39943|6|Mentioned|Table 11A|||||||||
11409|Maryborough Formation|39968|6|Mentioned|p80|||||||||
11409|Maryborough Formation|40245|6|Mentioned|Table 1|||||||||
11409|Maryborough Formation|40623|5|Briefly described|p54|||||||||
11409|Maryborough Formation|41057|6|Mentioned|p61|||||||||
11409|Maryborough Formation|41265|6|Mentioned|Map legend|Cretaceous||||||||
11409|Maryborough Formation|41736|6|Mentioned|Fig.1|||||||||
11409|Maryborough Formation|42282|6|Mentioned|p15|Cretaceous||||||||
11409|Maryborough Formation|42616|4|Described|p7|||||||||
11409|Maryborough Formation|42636|5|Briefly described|p9|||||||||
11409|Maryborough Formation|42894|2|Defined|p29|middle Cretaceous|Early Cretaceous|see also Fig.2 P22.||||||14-AUG-08
11409|Maryborough Formation|43008|5|Briefly described|map legend|||||||||
11409|Maryborough Formation|43059|4|Described|Table 1|||See also p10.||||||14-AUG-08
11409|Maryborough Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
11409|Maryborough Formation|43995|14|Not recorded|p8,Tb.p10,36,Fig.12||Aptian|Early Aptian||||||
11409|Maryborough Formation|44082|6|Mentioned|p14,22,24,Tb.p34||Aptian|(Early Aptian) Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
11409|Maryborough Formation|44091|14|Not recorded|p63||Cretaceous|||||||
11409|Maryborough Formation|44117|14|Not recorded|p23|||||||||
11409|Maryborough Formation|44128|14|Not recorded|Tb.1,p426|||||||||
11409|Maryborough Formation|44240|2|Defined|p333-340||Early Cretaceous|||||||
11409|Maryborough Formation|44241|14|Not recorded|p1,5-8,12,13,30,|||Fig.1, Tb.4.  Formerly "beds" defined above Graham's Creek Formation and below Burrum Coal Measures.||||||
11409|Maryborough Formation|44250|14|Not recorded|p90|||See also Lexicon.||||||
11409|Maryborough Formation|44360|14|Not recorded|p36||Early Cretaceous|||||||
11409|Maryborough Formation|44376|14|Not recorded|p12,15,2-24|||||||||
11409|Maryborough Formation|44380|14|Not recorded|p94|||||||||
11409|Maryborough Formation|44385|14|Not recorded|p5,10,11|||||||||
11409|Maryborough Formation|44386|14|Not recorded|p13|||||||||
11409|Maryborough Formation|44593|14|Not recorded|p23|||||||||
11409|Maryborough Formation|44616|14|Not recorded|p32,33,35|Early Cretaceous|Aptian|Quartz sandstone, mudstone, siltstone shale, conglomerate, thin limestone. low porosity.||||||
11409|Maryborough Formation|44648|14|Not recorded|p2|||||||||
11409|Maryborough Formation|44697|14|Not recorded|p91|||||||||
11409|Maryborough Formation|44750|14|Not recorded|p12,16,17||Cretaceous|||||||
11409|Maryborough Formation|44752|14|Not recorded|Fig.42,p298||Cretaceous|||||||
11409|Maryborough Formation|44753|14|Not recorded|p47,49,52-55||Early Cretaceous|Unconformably overlies Graham's Creek Formation.||||||
11409|Maryborough Formation|44754|14|Not recorded|p13||Early Triassic|||||||
11409|Maryborough Formation|44783|14|Not recorded|p2,47|||||||||
11409|Maryborough Formation|44794|14|Not recorded|p20|||||||||
11409|Maryborough Formation|44821|14|Not recorded|p33,35||Early Cretaceous|||||||
11409|Maryborough Formation|44852|14|Not recorded|p78||Early Cretaceous|||||||
11409|Maryborough Formation|44903|14|Not recorded|p20|||||||||
11409|Maryborough Formation|45107|6|Mentioned|p6|||||||||
11409|Maryborough Formation|45110|6|Mentioned|p147|||||||||
11409|Maryborough Formation|45440|4|Described|p.2,6,7,14,32,33-88||Aptian|Tb.1. Of many pages.||||||
11409|Maryborough Formation|60281|5|Briefly described|pvii, p36, Fig.30 App.1|Early Cretaceous|Early Cretaceous|Mudstone, shale, siltstone and sandstone with minor conglomerate, waterlaid tuff, coal and dense limestone. Contains the Gregory Sst Mbr and Cherwell Mudst Mbr.  Unconformably overlies Tiaro C. M.; conformably overlain by Burrum C.M.Max. thick: 2.4km.||||||14-AUG-08
11409|Maryborough Formation|61611|5|Briefly described|p264, p266, p267,p265 Fig. 3|Early Cretaceous|Early Cretaceous|Thickness: 2500m. Mainly marine and coastal/esturine/lacustrine sediments. Geological Province: Maryborough Basin.||||||13-MAR-09
11409|Maryborough Formation|62594|5|Briefly described|p546 Fig. 3, p559|Early Cretaceous|Late Jurassic|Shallow marine siliciclastic deposits. Age is largely Aptian. Geological Province: Maryborough Basin||||||09-AUG-06
11409|Maryborough Formation|63821|4|Described|p24|Early Cretaceous|Early Cretaceous|Overlain by Burrum Coal Measures. Geological Province: Maryborough Basin. Has a series of silicified beds at top and bottom. Comprises mudstone, shale, siltstone, sandstone, minor conglomerate, water-laid tuff and dense limestone. See also p12, p22, p37.||||||07-FEB-11
11409|Maryborough Formation|64665|5|Briefly described|p53 Fig.2.|Early Cretaceous|Early Cretaceous|Maryborough Basin.||||Is overlain by Burrum Coal Measures.||
11409|Maryborough Formation|64714|6|Mentioned|p9|||Underlie the Burrum Coal Measures.||||||
11409|Maryborough Formation|65452|6|Mentioned|p6 Fig.2|Cretaceous|Cretaceous|||||||
11409|Maryborough Formation|67402|4|Described|p165 tbl LPB1, p234|Albian|Aptian|Maryborough Basin. Deposited in a shallow marine setting. Up to 1800m thick. See also p235, p236 fig MRY4, p237.|||Includes the Gregory Sandstone.|Overlain by the Burrum Coal Measures.|Siltstone, mudstone, sandstone with minor conglomerate, liemstone and coal.|
11409|Maryborough Formation|68319|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Maryborough Basin||||Unconformably overlain by the Elliott Formation. Unconformably underlain by Myrtle Creek Sandstone.|Mudstone, siltstone, shale, labile sandstone, glauconitic sandstone; silicified siltstone to mudstone.|
11409|Maryborough Formation|68332|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Maryborough Basin.|||||Mudstone, siltstone, shale, labile sandstone, glauconitic sandstone; silicified siltstone to mudstone.|
11409|Maryborough Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Maryborough Basin.||||Is overlain conformably by Burrum Coal Measures.||
11409|Maryborough Formation|68679|6|Mentioned|p312-313|Cretaceous|Cretaceous|Northern New England Orogen.||||||
11409|Maryborough Formation|69582|5|Briefly described|p48, p50, p53|Early Cretaceous|Early Cretaceous|Maryborough Basin. Shallow marine rocks. Thermal conductivity is provided. Intersected in GSQ Maryborough 16. Estimated to be approximately 1400m thick.|||Includes the Gregory Sandstone member.|Unconformably overlies the Grahams Creek Formation.|Mudstone, shale, siltstone and sandstone.|
11409|Maryborough Formation|69594|5|Briefly described|p519, p548-550|Aptian|Aptian|Hawthorne (1960); Cranfield (1993). Maryborough Basin. Fluviatile followed by marine deposits. Resistant siltstones at top and bottom are persistent marker beds. Sedimentary features elaborated. Thickness variable: <610m to 2440m. Basal conglomerate derived from Grahams Creek Formation. Had a small gas flow in SDA Gregory River 1.||||Disconformably/unconformably overlies Grahams Creek Formation or Tiaro Coal Measures. Is overlain by Burrum Coal Measures.|Mudstone (quartz, clay and iron oxides, plant fragments, decalcified moulds of bivalves), shale, siltstone and sandstones (feldspathic greywackes, grey, green, thick-bedded, poorly sorted) with minor conglomerate, waterlaid tuff and dense limestone.|
11409|Maryborough Formation|69599|6|Mentioned|p587|||||||Is overlain unconformably by the Takura beds.||
11409|Maryborough Formation|72297|6|Mentioned|p748|||Maryborough Basin. Gas shows recorded from SDA Gregory River 1 and POG Gregory River 2 wells. Problems with potential reservoirs mentioned.||||||
11409|Maryborough Formation|73422|6|Mentioned|p3|Aptian|Aptian|Maryborough Basin. Aptian in age based on palynological and macrofossil records.||||Underlain by Grahams Creek Formation.||
11417|Maryland Granite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
11417|Maryland Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
11417|Maryland Granite|32492|6|Mentioned|Map legend|Triassic|Late Permian|Upper Permian or Triassic||||||
11417|Maryland Granite|32876|6|Mentioned|Map legend|Early Triassic|Late Permian|Upper Permian to Lower Triassic.||||||27-OCT-08
11417|Maryland Granite|32880|4|Described|p3|||See also p11. Upper Permian or Lower Triassic.||||||12-DEC-07
11417|Maryland Granite|33476|2|Defined|p70|Permian|Permian|Mention p50. Permian - Triassic||||||19-NOV-07
11417|Maryland Granite|33766|6|Mentioned|Map legend|Early Triassic|Permian|Permian - Early Triassic||||||
11417|Maryland Granite|35257|6|Mentioned|Fig.5|||||||||
11417|Maryland Granite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
11417|Maryland Granite|43008|5|Briefly described|map legend|||||||||
11417|Maryland Granite|44625|14|Not recorded|p383|||||||||
11417|Maryland Granite|48940|5|Briefly described|p70|||Refers Saint-Smith (1911).||||||27-OCT-08
11417|Maryland Granite|61789|5|Briefly described|p306|||Mineralogically separate to Maryland River Quartz Monzogranite. Has abundant mafic enclaves.||||||
11417|Maryland Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Medium grey, medium-grained, uneven-grained to slightly porphyritic (allanite-titanite-) hornblende-biotite monzogranite; mafic inclusions common; high magnetic response.||||||11-DEC-07
11417|Maryland Granite|63748|3|Fully described|p35, p42|Late Permian|Permian|The only granite in the Maryland Suite. Intrudes Silverwood Group, faulted against Stanthorpe Granite; unconformably overlain by Marburg Formation. Medium grey, medium-grained, uneven grained to slightly porphyritic monzogranite. See also p29 Fig. 33, p86||||||07-FEB-11
11417|Maryland Granite|69639|4|Described|p1, p6, p8, p74, p151-p156|Lopingian|Lopingian|New England Orogen. SHRIMP age is interpreted as a magmatic crystallisation age. Sample locality, petrography, and geochronology is described. See also p217, p220, p222, p238.|252.4 +/- 1.5 Ma|Maryland Suite||Intrudes the Silverwood Group. Faulted against and intruded by the Stanthorpe Granite. Intruded by the Cullendore Granite.|Grey, medium-grained, equigranluar granodiorite.|
11417|Maryland Granite|70876|5|Briefly described|p81|||Provided age is a SHRIMP U-Pb zircon date; an additional Rb-Sr biotite age of c. 242 Ma is provided from Shaw and Flood (1993).|252.4 +/- 1.5 Ma (Chisholm et al, 2014b)|||||
11417|Maryland Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|252+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
11417|Maryland Granite|71628|6|Mentioned|p19:97|||Flood (1970). After several variations, is now Maryland Granodiorite.||||||
11458|Matthews Pinnacle Quartz Diorite|22847|3|Fully described|p 56|Carboniferous|Middle Devonian|||||||
11458|Matthews Pinnacle Quartz Diorite|42633|5|Briefly described|Table 1 P7|||Reserved as Matthews Pinnacle Tonalite.||||||
11458|Matthews Pinnacle Quartz Diorite|42750|2|Defined|p46|Early Devonian||||||||
11458|Matthews Pinnacle Quartz Diorite|43093|4|Described|Appendix 1|Carboniferous|Middle Devonian|||||||
11458|Matthews Pinnacle Quartz Diorite|43259|4|Described|Appendix 1,p50.|Carboniferous|Devonian|Devonian-Carboniferous?||||||
11458|Matthews Pinnacle Quartz Diorite|43934|5|Briefly described|Map Legend||Devonian|||||||
11485|May Downs Gneiss|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1789+/-4Ma.||||||09-FEB-09
11485|May Downs Gneiss|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
11485|May Downs Gneiss|24308|5|Briefly described|p1003 Fig. 15|||||||||09-FEB-09
11485|May Downs Gneiss|24432|6|Mentioned|p565 Fig.4|||||||||
11485|May Downs Gneiss|32041|6|Mentioned|p352|||||||||
11485|May Downs Gneiss|32959|6|Mentioned|Fig.21|||||||||
11485|May Downs Gneiss|33900|6|Mentioned|Fig.1|||||||||
11485|May Downs Gneiss|35286|6|Mentioned|Fig.17|||||||||
11485|May Downs Gneiss|37862|6|Mentioned|p586|||||||||
11485|May Downs Gneiss|38232|6|Mentioned|p83|||||||||
11485|May Downs Gneiss|38234|6|Mentioned|p103|||||||||
11485|May Downs Gneiss|39362|6|Mentioned|Fig.1|||||||||
11485|May Downs Gneiss|40623|5|Briefly described|p103|||||||||
11485|May Downs Gneiss|41381|6|Mentioned|p325|||||||||
11485|May Downs Gneiss|41978|6|Mentioned|p497|||||||||
11485|May Downs Gneiss|41979|6|Mentioned|p538|||||||||
11485|May Downs Gneiss|42503|6|Mentioned|p335|||||||||
11485|May Downs Gneiss|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Haslingden Group. Gneiss, schist.||||||09-FEB-09
11485|May Downs Gneiss|43608|6|Mentioned|Fig.11,p11|||||||||
11485|May Downs Gneiss|45161|6|Mentioned|p10|||||||||
11485|May Downs Gneiss|46801|6|Mentioned|p115|||See also Fig. 14||||||
11485|May Downs Gneiss|49009|6|Mentioned|p48|||||||||
11485|May Downs Gneiss|61922|5|Briefly described|p8, p9 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: <1789+/-4Ma.  Geological Province: Mount Isa Inlier/Western Fold Belt. See also p20 Fig.12.||||||07-NOV-08
11485|May Downs Gneiss|61929|5|Briefly described|p128 Fig. 2|||||||||
11485|May Downs Gneiss|61933|6|Mentioned|p181, p183|||||||||
11485|May Downs Gneiss|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt. Thickness >500m.||||||
11485|May Downs Gneiss|63866|5|Briefly described|p58-p59|Statherian|Statherian|Leichhardt Superbasin. A pegmatite dyke within this unit records a U-Pb SHRIMP monazite age of 1584+/- 3 Ma (Page, OZCHRON)|1789 +/- 4 Ma (maximum depositional age)|||||
11485|May Downs Gneiss|64250|6|Mentioned|p11 fig 3, p22|||Western Fold Belt, Mount Isa Inlier. Appears as May Downs Granite in Fig.7.|<1789 +/- 4 Ma|||||
11485|May Downs Gneiss|64744|5|Briefly described|p355 Fig.5, pp359-362.|||Mount Isa terrane. Part of the basement. Of uncertain age and stratigraphic affinities. Shown as pre-1800 Ma basement.|||||Variably migmatised cordierite-potash feldspar gneiss; locally altered to sillimanite-biotite-potassium feldspar gneiss.|
11485|May Downs Gneiss|65396|6|Mentioned|p82, p175, p194-195, p241|Statherian|Statherian|Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform. Detrital zircon sources listed.|1789 +/- 4 Ma|Haslingden Group.||||
11485|May Downs Gneiss|66824|6|Mentioned|p135, 148|||Anatexis occurred during low-P high-T metamorphism.||||||
11485|May Downs Gneiss|67499|6|Mentioned|p941, p940 Fig.3|||Intruded by the Sybella batholith  around 1657 +/- 7 Ma||||||
11485|May Downs Gneiss|69222|6|Mentioned|p221, p222 Fig.2|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform. Metamorphosed during the 1890-1840 Ma Barramundi Orogeny.||||||
11485|May Downs Gneiss|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
11485|May Downs Gneiss|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1789+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Gneiss, pegmatite.|
11485|May Downs Gneiss|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|||||Metamorphics.|
11533|McCord Granite|23291|5|Briefly described|p101 Tb. 3.12|Late Carboniferous|Late Carboniferous|Intrudes Saucebottle Granite (Ootann Supersuite); intruded by Crystalbrook Volcanic Neck. Southern part is named Roberts Creek granite (Champion, 1991). Age: 309 Ma (Richards et al, 1966); 321 (Black, 1978). Geological Province: Georgetown Region.||||||07-APR-15
11533|McCord Granite|23500|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|O'Briens Creek Supersuite.||||||
11533|McCord Granite|23501|5|Briefly described|map legend|Late Carboniferous|Late Carboniferous|O'Briens Creek Supersuite.||||||
11533|McCord Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 312. I-Type.||||||
11533|McCord Granite|23616|6|Mentioned|Fig 4 p27|||Of O'Briens Creek Supersuite.||||||
11533|McCord Granite|24485|5|Briefly described|p5, p54 Tb.8|Late Carboniferous|Late Carboniferous|Age: ~321Ma (Rb-Sr, biotite) and 321 +/- 4Ma (U-Pb SHRIMP zircon). Parent: O'Briens Creek Supersuite||||||
11533|McCord Granite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Of the O'Briens Creek Supersuite.||||||
11533|McCord Granite|42691|5|Briefly described|map legend|Paleozoic||Reserved as McCord Adamellite.||||||07-NOV-08
11533|McCord Granite|43060|5|Briefly described|p94|||of O'Briens Creek Supersuite||||||
11533|McCord Granite|43083|4|Described|p125|||Of O'Briens Creek Supersuite. Ages: 309 Ma and 321 Ma. mainly medium-grained, even-grained to slightly porphyritic adamellite.||||||17-JUN-09
11533|McCord Granite|43087|2|Defined|p21|Late Carboniferous||Isotopic ages 309Ma, 321Ma. O'Briens Creek Supersuite.||||||
11533|McCord Granite|43110|6|Mentioned|p46|||||||||
11533|McCord Granite|43259|4|Described|Appendix 1,p38.||Carboniferous|||||||
11533|McCord Granite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
11533|McCord Granite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province.||Unit in O'Briens Creek Supersuite.|||Pale pink to cream, medium-grained, equigranular to moderately porphyritic biotite granite; commonly altered.|
11533|McCord Granite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province||Of the O'Briens Creek Supersuite.|||Pale pink to cream, medium grained, equigranular to slightly porphyritic, biotite granite.|
11534|McDevitt Metamorphics|22533|6|Mentioned|p54|Statherian|Statherian|placed in Forsyth subprovince||||||
11534|McDevitt Metamorphics|23085|6|Mentioned|p669|||||||||
11534|McDevitt Metamorphics|23220|6|Mentioned|Fig.1|||of Forsayth Subprovince.||||||
11534|McDevitt Metamorphics|23291|3|Fully described|p22, p87 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Geological Province: Georgetown Region.||||||08-JUL-15
11534|McDevitt Metamorphics|23430|5|Briefly described|p451|||||||||
11534|McDevitt Metamorphics|23431|5|Briefly described|p530|||Geological Province Forsayth Subprovince||||||
11534|McDevitt Metamorphics|23453|5|Briefly described|p10 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11534|McDevitt Metamorphics|23496|5|Briefly described|Table 1||Proterozoic|||||||
11534|McDevitt Metamorphics|23500|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11534|McDevitt Metamorphics|23510|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
11534|McDevitt Metamorphics|23616|5|Briefly described|Table 1C p15, p24||Proterozoic|Age: Proterozoic; recent SHRIMP dating of equivalent units in Georgetown Region suggests an age of ~1650 Ma. Unconformably overlain by Scardons Volcanic Group and Gilbert River Formation. Dargalong Inlier.||||||
11534|McDevitt Metamorphics|23713|5|Briefly described|p11|||Correlate with rock in the Robertson River Subgroup. Dargalong Province.||||||
11534|McDevitt Metamorphics|24197|5|Briefly described|p76|Paleoproterozoic|Paleoproterozoic|Geological Province: Georgetown Inlier (Etheridge Province/Forsayth Subprovince).||||||07-FEB-11
11534|McDevitt Metamorphics|24485|3|Fully described|p15 Tb.1|Mesoproterozoic|Mesoproterozoic|Age: ~1700-1655Ma. Intruded by the Cobbold Metadolerite. Geological Province: Forsayth Subprovince||||||
11534|McDevitt Metamorphics|24486|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Forsayth Sub-province (Etheridge Province).||||||07-NOV-08
11534|McDevitt Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11534|McDevitt Metamorphics|32528|5|Briefly described|Table 1|||||||||
11534|McDevitt Metamorphics|37570|4|Described|p122|||See also Fig.3||||||
11534|McDevitt Metamorphics|39445|5|Briefly described|p46|||||||||
11534|McDevitt Metamorphics|40892|5|Briefly described|p71|||||||||
11534|McDevitt Metamorphics|41680|6|Mentioned|p119|||||||||
11534|McDevitt Metamorphics|42304|6|Mentioned|p14||Precambrian|||||||
11534|McDevitt Metamorphics|42658|5|Briefly described|p21|||Precambrian||||||
11534|McDevitt Metamorphics|42681|6|Mentioned|p17|||||||||
11534|McDevitt Metamorphics|42691|5|Briefly described|map legend|Precambrian||||||||
11534|McDevitt Metamorphics|43060|3|Fully described|p27,Table 1c|||||||||
11534|McDevitt Metamorphics|43083|3|Fully described|p18 Tb. 1, p24|||Unconformable below Gilbert River Formation. Gradational contact with Dargalong metamorphics; intruded by Carrs and McCord Granites. Probable Early Proterozoic age. Geological province: Hodgkinson Province. Detailed lithology included.||||||17-JUN-09
11534|McDevitt Metamorphics|43087|6|Mentioned|p8|||||||||
11534|McDevitt Metamorphics|43110|4|Described|Table 1.|||?Proterozoic age||||||
11534|McDevitt Metamorphics|43287|6|Mentioned|Map Legend|Mesoproterozoic|Paleoproterozoic|of Yambo Metamorphic Group.||||||07-NOV-08
11534|McDevitt Metamorphics|43596|6|Mentioned|p6 Fig. 6|||Geological province: Yambo province.||||||27-JAN-09
11534|McDevitt Metamorphics|43665|5|Briefly described|p14||Proterozoic|||||||
11534|McDevitt Metamorphics|43896|14|Not recorded|Map Legend||Proterozoic|||||||
11534|McDevitt Metamorphics|44246|5|Briefly described|Map Legend||Proterozoic|||||||
11534|McDevitt Metamorphics|44296|14|Not recorded|Map Legend||Proterozoic|||||||
11534|McDevitt Metamorphics|44926|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
11534|McDevitt Metamorphics|45025|3|Fully described|p23-4||Precambrian|||||||
11534|McDevitt Metamorphics|50537|6|Mentioned|p1.1|||Geological Province: Georgetown Inlier.||||||
11534|McDevitt Metamorphics|63866|5|Briefly described|p75, p77, p81|||Forsayth Subprovince, Etheridge Province. Suggested to correlate either with the Etheridge or Dargalong Metamorphics Group.|||||Laminated to thin-bedded metapelites and subordinate meta-arenite, quartzite and mafic sills.|
11534|McDevitt Metamorphics|65887|5|Briefly described|p40 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
11534|McDevitt Metamorphics|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||||||
11534|McDevitt Metamorphics|68405|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Etheridge Province.|||Informally subdivided into two units.|Older than Fig Tree Hill Granite Complex.|Dark grey to black, foliated to massive amphibolite, metadolerite; mainly (garnet-) muscovite-biotite schist and gneiss, migmatite, minor amphibolite, leucogranite.|
11534|McDevitt Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province. This unit, as well as the Robertson River Subgroup, Cassidy Creek and Juntala Metamorphics, are all mapped under the symbol, -Per.||Unit in Etheridge Group.||||
11534|McDevitt Metamorphics|69591|5|Briefly described|p61, p65-66, p83|Paleoproterozoic|Paleoproterozoic|Georgetown Inlier, Forsayth Subprovince, Etheridge Province. West of Chillagoe. Upper greenschist to lower amphibolite grade metamorphism. Grades into Dargalong Metamorphics. Not directly dated.||||Adjacent to Dargalong Metamorphics. Probably correlative with Robertson River Subgroup. Is intruded by Fig Tree Hill Granite and Lyndbrook Complex.|Mainly laminated to thin-bedded metapelites (mica schist) and subordinate micaceous quartzose meta-arenite and quartzite; mafic sills and irregular pod-like bodies are interlayered throughout the succession.|
11534|McDevitt Metamorphics|72983|6|Mentioned|p15|Mesoproterozoic|Paleoproterozoic|||||||
11575|McNamara Group|7071|5|Briefly described|p1|Mesoproterozoic|Paleoproterozoic|Geological Province: northern Mount Isa Inlier.||||||07-NOV-08
11575|McNamara Group|22438|6|Mentioned|p549, Fig.12|||||||||
11575|McNamara Group|22453|5|Briefly described|p 11|||NT and QLD||||||
11575|McNamara Group|22457|6|Mentioned|Fig29 P30|||||||||
11575|McNamara Group|22468|5|Briefly described|p 16, 17|||||||||
11575|McNamara Group|22585|6|Mentioned|Fig1 P736|||||||||
11575|McNamara Group|22644|5|Briefly described|5 fig 2|||Geol. province: Mount Isa Basin. Underlain by Fiery Creek Volcanics.||||||06-NOV-06
11575|McNamara Group|22665|6|Mentioned|P219, P227|||||||||
11575|McNamara Group|22680|5|Briefly described|83,85-87|Mesoproterozoic|Paleoproterozoic|Geol. province: Mount Isa Basin.||||||07-NOV-08
11575|McNamara Group|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological  province: Mount Isa Fold Belt.||||||07-NOV-08
11575|McNamara Group|23072|6|Mentioned|p754|||||||||
11575|McNamara Group|23073|5|Briefly described|p744|||||||||
11575|McNamara Group|23075|5|Briefly described|p730||Mesoproterozoic|Age: 1595+/-6 M yr.||||||06-NOV-06
11575|McNamara Group|23198|5|Briefly described|p873, 875||Paleoproterozoic|Age: Late Palaeoproterozoic. Informally referred to 'Lower McNamara Group".||||||07-NOV-08
11575|McNamara Group|23362|6|Mentioned|337|||||||||
11575|McNamara Group|23387|6|Mentioned|p18 fig.19|||||||||
11575|McNamara Group|23393|5|Briefly described|p11, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
11575|McNamara Group|23395|6|Mentioned|p383|||||||||
11575|McNamara Group|23396|5|Briefly described|p407 Fig.2|||||||||
11575|McNamara Group|23397|5|Briefly described|p463|||||||||
11575|McNamara Group|23398|5|Briefly described|p441|||||||||
11575|McNamara Group|23399|5|Briefly described|p487|||||||||
11575|McNamara Group|23405|4|Described|p566|||Lawn Hill Platform.||||||
11575|McNamara Group|23406|5|Briefly described|p601 Fig. 3, p603-4, p607 Fig. 8|||Includes 11 named formations (see p607 Fig. 8). Geological province: Isa Superbasin.  Lower part is of ramp carbonates and clastics; upper is clastics.||||||22-JUL-13
11575|McNamara Group|23408|5|Briefly described|p509, p513 Fig. 2|||Previous interpretations of this group are included. Comprises: Torpedo Ck. Quartzite, Gunpowder Ck., Paradise Ck., Esperanza, Lady Loretta Fms., Shady Bore Quartzite, Riversleigh and Lawn Hill Fms (Hutton et al 1981). On Lawn Hill Platform||||||15-JUN-09
11575|McNamara Group|23409|4|Described|p537|||Of Lawn Hill Platform.||||||21-SEP-06
11575|McNamara Group|23448|5|Briefly described|p479|||||||||
11575|McNamara Group|23466|5|Briefly described|p267|||||||||
11575|McNamara Group|23518|4|Described|p9 Fig. 3, p12|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
11575|McNamara Group|23957|6|Mentioned|p1123|||||||||
11575|McNamara Group|23958|4|Described|p1132|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
11575|McNamara Group|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
11575|McNamara Group|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
11575|McNamara Group|23986|5|Briefly described|p65|||||||||21-SEP-06
11575|McNamara Group|24034|5|Briefly described|p9|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Quartzite, siltstone, stromatolitic dolomite, laminated siltstone, dolomitic siltstone, orthoquartzite, shale and fine-grained sandstone.||||||
11575|McNamara Group|24308|5|Briefly described|p990, p987 Fig.2|Mesoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Superbasin||||||07-NOV-08
11575|McNamara Group|24309|5|Briefly described|p1013|||||||||
11575|McNamara Group|24419|5|Briefly described|p12 Fig.4, p13 Fig.5, p14, p17|Paleoproterozoic|Paleoproterozoic|Includes the Gunpowder Creek Formation. In URANDANGI 1:250 000 sheet area the McNamara Group is represented by the upper Gunpowder Creek Formation. Unconformably overlies Yaringa Metamorphics. Geol.Prov: Isa Superbasin.||||||07-NOV-08
11575|McNamara Group|24432|5|Briefly described|p562 Fig.2|Calymmian|Statherian|Geological Province: Lawn Hill Platform.||||||28-JAN-05
11575|McNamara Group|24442|6|Mentioned|p22, p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Includes Lawn Hill, Plain Creek, Formations, Shady Bore Quartzite and Musselbrook Formation.  Age: 1670-1600Ma.  Geological Province: McArthur Basin.||||||
11575|McNamara Group|30534|6|Mentioned|p300|||See also p305.||||||21-SEP-06
11575|McNamara Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|33900|6|Mentioned|p4|||||||||
11575|McNamara Group|35074|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|36548|6|Mentioned|p513|||||||||
11575|McNamara Group|37459|2|Defined|p426|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
11575|McNamara Group|37462|4|Described|Table4.VII|||||||||
11575|McNamara Group|37565|6|Mentioned|Fig.5|||||||||
11575|McNamara Group|37568|4|Described|p84|||||||||
11575|McNamara Group|37569|6|Mentioned|p91|||||||||
11575|McNamara Group|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|38232|6|Mentioned|p82|||||||||
11575|McNamara Group|38234|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|38235|6|Mentioned|p117|||||||||
11575|McNamara Group|38237|4|Described|p127|||||||||
11575|McNamara Group|38276|6|Mentioned|Fig.1|||||||||
11575|McNamara Group|38278|6|Mentioned|Fig.1|||||||||
11575|McNamara Group|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|38348|4|Described|p5|||||||||
11575|McNamara Group|38350|4|Described|p15|||||||||
11575|McNamara Group|38584|6|Mentioned|p17|||||||||
11575|McNamara Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|38835|6|Mentioned|p164|||||||||
11575|McNamara Group|38836|6|Mentioned|p165|||||||||
11575|McNamara Group|38919|6|Mentioned|p496|||||||||
11575|McNamara Group|39043|6|Mentioned|p10|||||||||
11575|McNamara Group|39338|6|Mentioned|p351|||See also Fig.1.||||||
11575|McNamara Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Lawn Hill, Plain Creek and Musselbrook Formations.||||||10-JAN-05
11575|McNamara Group|39445|4|Described|p41|||Carp. Shallow marine. Lawn Hill Platform. See also pp36,55,56 and Table 2.||||||21-SEP-06
11575|McNamara Group|39492|6|Mentioned|p31|||||||||
11575|McNamara Group|39497|4|Described|p11|||||||||
11575|McNamara Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||15-JUN-06
11575|McNamara Group|39622|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|39925|6|Mentioned|p329|||See also Fig.2.||||||
11575|McNamara Group|39934|6|Mentioned|p317|||See also Fig.3.||||||
11575|McNamara Group|39944|6|Mentioned|p228|||||||||
11575|McNamara Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
11575|McNamara Group|40221|3|Fully described|p13|||||||||
11575|McNamara Group|40394|6|Mentioned|Fig.2|||||||||
11575|McNamara Group|40840|6|Mentioned|Map legend|||||||||
11575|McNamara Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
11575|McNamara Group|41307|5|Briefly described|p16|||||||||
11575|McNamara Group|41381|6|Mentioned|p325|||||||||
11575|McNamara Group|41862|6|Mentioned|p474|||||||||
11575|McNamara Group|41978|6|Mentioned|p502|||||||||
11575|McNamara Group|41979|5|Briefly described|p514|||||||||
11575|McNamara Group|42367|4|Described|p18||Proterozoic|Correlated with Mount Isa Group.||||||18-JAN-07
11575|McNamara Group|42565|5|Briefly described|Table 1 P5, P4|||||||||
11575|McNamara Group|42706|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1870Ma. Dolomite, siltstone, chert, sandstone, conglomerate.||||||09-FEB-09
11575|McNamara Group|42766|5|Briefly described|p1|||||||||
11575|McNamara Group|42819|5|Briefly described|p312|||||||||
11575|McNamara Group|43107|6|Mentioned|p8|||||||||
11575|McNamara Group|43235|6|Mentioned|p8|||Proterozoic||||||
11575|McNamara Group|43486|5|Briefly described|21|||||||||
11575|McNamara Group|43608|6|Mentioned|Fig.11,p11|||||||||
11575|McNamara Group|43615|6|Mentioned|p13|||||||||
11575|McNamara Group|43616|6|Mentioned|p2|||||||||
11575|McNamara Group|43652|6|Mentioned|p388|||||||||
11575|McNamara Group|44195|6|Mentioned|p350|||||||||
11575|McNamara Group|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
11575|McNamara Group|45161|4|Described|p12|||||||||
11575|McNamara Group|45166|4|Described|p29|||||||||
11575|McNamara Group|46598|5|Briefly described|p307|||||||||
11575|McNamara Group|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
11575|McNamara Group|46960|6|Mentioned|p216|||||||||
11575|McNamara Group|47083|3|Fully described|p14-18||Proterozoic|Age: 1470-1490 Ma upper age limit. Correlates with Mount Isa Group. Unconformably overlain by Thorntonia Fm; unconformably underlain by Surprise Crk Fm. Max thickness: 4000 m.||||||21-SEP-06
11575|McNamara Group|49018|6|Mentioned|p6|||||||||
11575|McNamara Group|49041|5|Briefly described|Table 1|||||||||
11575|McNamara Group|50225|5|Briefly described|p406 Fig. 10, p407|Paleoproterozoic|Paleoproterozoic|Geological Province: Isa Superbasin.||||||07-FEB-11
11575|McNamara Group|50536|5|Briefly described|p11.3|Paleoproterozoic|Paleoproterozoic|Age: ~1670Ma.||||||07-NOV-08
11575|McNamara Group|50550|6|Mentioned|p1140|||Geological Province: Western Fold Belt.||||||19-DEC-07
11575|McNamara Group|50624|5|Briefly described|p234 Fig.2|Calymmian|Statherian|U-Pb ages: Upper: 1595 +/-6 Ma, Lower: 1653 +/-7 Ma.||||||22-JUL-13
11575|McNamara Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Gunpowder Creek Formation, Torpedo Creek Quartzite.||||||
11575|McNamara Group|60558|5|Briefly described|p3, p5 Fig. 4|||Includes eight units.||||||03-JUN-09
11575|McNamara Group|61262|5|Briefly described|p455 Fig. 11|Mesoproterozoic|Paleoproterozoic|Geological Province: western Mount Isa Block.||||||07-NOV-08
11575|McNamara Group|61736|5|Briefly described|p673|Paleoproterozoic|Paleoproterozoic|Includes the Riversleigh Siltstone. Depositional age range: 1653+/-7Ma and 1658+/-3Ma for tuffaceous units.||||||
11575|McNamara Group|61904|5|Briefly described|p132 Fig. 2|Proterozoic|Proterozoic|Includes Lawn Hill Formation as youngest section. Max. thickness: 10km. Fine-grained clastic sediments and minor volcanic rocks hosting base metal deposits of Mt. Isa, Hilton, Hilton North and Lady Loretta.||||||
11575|McNamara Group|61913|5|Briefly described|p161|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
11575|McNamara Group|61922|5|Briefly described|p9 Fig. 3, p10|Mesoproterozoic|Paleoproterozoic|Age: ~1660-1595Ma.  Geological Province: Mount Isa Inlier. See also p21 Fig.13.||||||07-NOV-08
11575|McNamara Group|61929|5|Briefly described|p128 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: 1653+/-7 to 1595+/-6Ma.||||||07-NOV-08
11575|McNamara Group|61936|5|Briefly described|p194 Fig. 6|Mesoproterozoic|Paleoproterozoic|Age: >1650-1600Ma.Shown to include Walford Dolomite, Mount Les Siltstone and Doomadgee Formation in figure; these also included in the correlating Fickling Group in the southern Murphy Inlier. Geol.Prov: Lawn Hill Platform, Western F.B., Mount Isa Inlier||||||07-NOV-08
11575|McNamara Group|62084|5|Briefly described|p936 Fig.5, p938|||Isa Superbasin. Lawn Hill. Hosts Mount Isa, Hilton and George Fisher deposits (Zn-Pb-Ag mineralisation).|||Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation, Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation|||
11575|McNamara Group|62473|5|Briefly described|p75||Paleoproterozoic|Contains the Riversleigh Formation. Age: ca. 1640Ma.||||||17-JUN-09
11575|McNamara Group|62535|5|Briefly described|p672-674|Statherian|Statherian|Lawn Hill Platform. Age of redeposited tuffaceous unit in the lower part of the Group.|1658 +/- 3 Ma.||Torpedo Creek, Shady Bore Quartzites; Gunpowder, Paradise Creek, Esperanza, Lady Loretta Formations; Mount Les, Riversleigh Siltstones.|||
11575|McNamara Group|62592|5|Briefly described|p73.|||Mount Isa Inlier. Upper parts are equivalent to the presumed deposition of topmost Willyama Supergroup, subsequently removed.||||||
11575|McNamara Group|62659|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
11575|McNamara Group|63023|5|Briefly described|p1025 Fig. 2|||Geological Province: Isa Superbasin.||||||
11575|McNamara Group|63113|5|Briefly described|p1214 Fig.2.|||Isa Superbasin.|c.1659-c.1589 Ma.||Includes Shady Bore and Torpedo Creek Quartzites; Riversleigh Siltstone; Lady Loretta, Esperanza, Paradise Creek, Gunpowder Creek, Termite Range and Lawn Hill Formations.|||
11575|McNamara Group|63114|6|Mentioned|p1252.|||Lawn Hill platform, Isa superbasin.|||||Carbonate, carbonaceous siltstone, shale.|
11575|McNamara Group|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt.|Between c.1700 and 1670 Ma.|||Is intruded by Sybella Granite.|Siltstone, sandstone, shale.|
11575|McNamara Group|63866|6|Mentioned|p52|||||||||
11575|McNamara Group|63884|5|Briefly described|p14|||Predominantly sideritic and locally carbonaceous shale, mudstone and sandstone.||||||
11575|McNamara Group|64137|6|Mentioned|p1544|||McArthur River area. Same age as Tarcoola Formation.||||||
11575|McNamara Group|64250|6|Mentioned|p25 fig 10, p19, p24|||Western Fold Belt, Mount Isa Inlier.|c.1660 Ma - 1595 +/- 6 Ma|||||
11575|McNamara Group|64317|6|Mentioned|p588, p601|||||||||
11575|McNamara Group|64724|5|Briefly described|p45 Fig.5, p46|Calymmian|Statherian|Lawn Hill Platform / Mt Isa Inlier unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||02-APR-12
11575|McNamara Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
11575|McNamara Group|64743|6|Mentioned|p342. |Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier. A sequence of sag-phase sediments up to c.8 km thick.|1650-1590 Ma.|||Equivalent to Paragon Group, Broken Hill Block.||
11575|McNamara Group|64744|5|Briefly described|p353 Fig.4, p354. ||Statherian|Mount Isa Basin.|||||Fluviatile to shallow marine sandstones, siltstones and dolostones; lesser intercalated black shale.|
11575|McNamara Group|64815|6|Mentioned|p3, |||||||||
11575|McNamara Group|65209|6|Mentioned|p38|||||||correlates with Namerinni Group||
11575|McNamara Group|65228|6|Mentioned|p8, p16|Proterozoic||Most complete stratigraphic sections in Lawn Hill Platform area. Contains cauliflower chert nodules and other ?evaporite pseudomorphs.||||||
11575|McNamara Group|65337|4|Described|p v, p6 Fig.3.  |Mesoproterozoic|Paleoproterozoic|Deposited in a variety of shallow-marine settings.|c.1670-1590 Ma.||Has Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Drummond, Brumby, Plain Creek, Termite Range, Lawn Hill Formations; Shady Bore Quartzite, Riversleigh Siltstone and Bullrush Conglomerate|Disconformably, locally unconformably, overlies Surprise Creek Formation.|Mixed succession of siliciclastic and carbonate rocks: shallow-marine sandstone, red-beds,stromatolitic and evaporitic dolostone and chert; fan delta sandstone and conglomerate; mudstone, siltstone and minor dolostone.|
11575|McNamara Group|65387|6|Mentioned|p85|||Widespread volcanism around 1690-1650 Ma is evident from tuff layers in this unit and the Mount Isa Group.||||||
11575|McNamara Group|65396|5|Briefly described|p82, p175, p188, p197, p241, p439|Calymmian|Statherian|Isa Superbasin: Western Fold Belt. Hosts giant shale-hosted Pb-Zn-Ag+/-Cu deposits.|1660 - 1595 +/- 6 Ma||Lower and Upper Gunpowder Creek Formation, Paradise Creek, Esperanza, Lady Loretta, Riversleigh, Termite Range, Lawn Hill Formations; Shady Bore Quartzite.|||04-APR-17
11575|McNamara Group|66800|6|Mentioned|p933.|||Western Fold Belt, Mount Isa Inlier. Correlated with younger parts of Eastern Fold Belt on basis of SHRIMP data (Page and Sun 1998).||||||
11575|McNamara Group|66824|6|Mentioned|p133, 148|||Local occurrence of Sybella Granite pebbles in basal conglomerate.||||Is faulted against and unconformably overlies Sybella Granite. Equivalent to Mount Isa Group.||
11575|McNamara Group|66843|6|Mentioned|p36||||||Includes Lawn Hill Formation.|||12-SEP-19
11575|McNamara Group|66844|5|Briefly described|p244-245|||Lawn Hill and Gunpowder region. This paper concentrates on the lower part of this Group. SE-thickening, characterised by extensional or transtentional faults, deposited in an intracratonic rift basin.|||Includes Prize, Gun, Loretta, River, Term, Lawn, Wide and Doom Supersequences.|Unconformably overlies Fiery Creek Formation.||
11575|McNamara Group|67323|4|Described|p10-11, p26, p34-36, p39, p60, p107|||See also GIS attrib tbl, Solid Geology Map. Century, Mount Oxide, Camooweal-Murphy and Ardmore-May Downs Domains, Mount Isa Inlier. Formally subdivided and informally subdivided to show altered rocks as separate unit. The upper part of the Group (deposited ~1620-1595 Ma) contains the Lawn, Wide and Doom Supersequences. CONSTITUENTS (continued): Plain Creek Formation, Riversleigh Siltstone, Shady Bore Quartzite, Termite Range Formation, Torpedo Creek Quartzite.|~1660-1595 Ma.||Includes  Esperanza Formation, Gun Supersequence, Gunpowder Creek Formation, Lady Loretta Formation, Lawn Hill Formation, Mount Oxide Chert Member, Paradise Creek Formation. See COMMENTS for more.|Geophysics show that Yeldham Granite underlies.|Includes altered carbonate rocks - some leached, porous beds, some silicified and/or ferruginised|
11575|McNamara Group|67499|6|Mentioned|p939|||Occurs about 220km northwest of Mt Isa.||||Stratigraphically equivalent to the Mt Isa Group. Overlain by the South Nicholson Group.||08-MAY-12
11575|McNamara Group|67539|6|Mentioned|p14|||||||Unconformably overlain by Constance Sandstone, South Nicholson Group.||
11575|McNamara Group|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|Western Succession.||||Overlies Surprise Creek Formation.||
11575|McNamara Group|68146|6|Mentioned|p196|||||||Underlies South Nicholson Group.||
11575|McNamara Group|68542|6|Mentioned|p6|||Of Andrews (1998).|||Inclydes informal Lower and Upper McNamara Groups.|Is overlain unconformably by South Nicholson Group.||22-OCT-19
11575|McNamara Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
11575|McNamara Group|68576|5|Briefly described|Q_2: p6|||Andrews (1998).|||Lower and Upper McNamara Groups.|Is overlain unconformably by South Nicholson Group.||
11575|McNamara Group|68732|5|Briefly described|p159-162||||||Includes the Paradise Creek Formation, Esperanza Formation, and Lady Loretta Formation.||Contains braided fluvial cross-stratified quartzites and pebbly quartzites at or near its base.|01-DEC-17
11575|McNamara Group|69222|5|Briefly described|p221|Calymmian|Statherian|Lawn Hill Platform; across the Western Fold Belt it is called the Mount Isa Group. Age range c.1653-1595 Ma.|1653 +/- 7 Ma|||Overlies Surprise Creek Formation, Correlated with Mount Isa Group||09-FEB-18
11575|McNamara Group|69370|6|Mentioned|p307 Fig.2|Calymmian|Statherian|Western Fold Belt, Mount Isa Block.||||Is intruded by Sybella Granite.||25-JAN-19
11575|McNamara Group|69417|6|Mentioned|p2:5-6|Statherian|Statherian|South Nicholson/Lawn Hill Basin.||||||12-JUL-16
11575|McNamara Group|69433|4|Described|p18:2-3, 5-6, 8-10|Statherian|Statherian|Sweet and Hutton (1982), Hutton et al. (1981). Southern succession, Lawn Hill Platform. Hosts the world-class Century Zn-Pb-Ag deposit, in Qld, 60km E of the border. The unit's extension into NT should be considered prospective.|c.1690-1595 Ma (Page et al., 2000).||Drummond, Brumby, Plain Creek, Lawn Hill Formations; Bullrush Conglomerate; Shady Bore Quartzite.|Overlies Carrara Range Group unconformably, and Surprise Creek Formation disconformably or unconformably. Correlated with Fickling Group.|Sandstone, conglomerate, siltstone, shale and various carbonate rocks, commonly silicified to chert in outcrop.|12-JUL-16
11575|McNamara Group|69434|5|Briefly described|p19:4, 6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform. A possible correlative of Caulfield beds (South Nicholson Basin).||||Is overlain unconformably by Accident Subgroup (South Nicholson Group).||12-JUL-16
11575|McNamara Group|69443|6|Mentioned|p28:19|||Lawn Hill Platform.|||Lawn Hill Formation.|||12-JUL-16
11575|McNamara Group|69591|4|Described|p29, p41-44, p46, p54, p108|Paleoproterozoic|Paleoproterozoic|See also p109 Fig.2.106, p111. Lawn Hill Platform. Marks the onset of deposition in the Isa Superbasin.|~1650-1595 Ma.||Torpedo Creek, Shady Bore Quartzites; Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Lawn Hill, Termite Range, Plain Creek Formations; Riversleigh Siltstone.|Coeval with Mount Isa Group. The upper part is correlated with the Milo beds.|Arenites, argillites and carbonate platform rocks, followed by deepwater carbonaceous clastics. Uppermost sediments are fluvial.|
11575|McNamara Group|69673|6|Mentioned|p3 fig 2, p51|Calymmian|Statherian||1690-1595 Ma||Includes Widdallion Sandstone Member, Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Bullrush Conglomerate, Brumby Formation, Drummond Formation|Correlated with Fickling Group|Sandstone, conglomerate, siltstone, shale and various carbonate rocks which are commonly silicified to chert.|
11575|McNamara Group|70864|5|Briefly described|p75, 74 Fig 2|Mesoproterozoic|Paleoproterozoic||||Includes Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation, Shady Bore Quartzite||Dolomitic and carbonaceous siltstones.|
11575|McNamara Group|70897|5|Briefly described|p36-37, p39, p41-42, p45|Paleoproterozoic|Paleoproterozoic|Mixed carbonate-clastic lithofacies. Source of 1680 Ma zircons in Mullera Formation. Uppermost units deposited c.1590 Ma.|c.1640 Ma.|||Isa Superbasin. Is overlain unconformably by South Nicholson Group.||
11575|McNamara Group|71369|5|Briefly described|p4, p10-11, p24, p33, p36, p49|||Underwent moderate folding but little metamorphism during the 1585-1500 Ma Mount Isa Orogeny. Basement for South Nicholson Group.||||Is overlain unconformably by South Nicholson Group.||20-FEB-18
11575|McNamara Group|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin, and Lawn Hill Platform, Mount Isa Inlier.||||Underlain unconformably by Carrara Range Group. Equivalent to McNamara Group.||
11575|McNamara Group|71960|6|Mentioned|p85, p86 Fig. 8|||||||Shown as equivalent to Mount Isa Group.||
11575|McNamara Group|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Lawn Hill Formation.|||
11575|McNamara Group|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Lawn Hill Formation.|||
11575|McNamara Group|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Lawn Hill Formation, Termite Range Formation.|||
11575|McNamara Group|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series. Includes the Wide Supersequence, Lawn Supersequence and the Term Supersequence-3.|||Includes Lawn Hill Formation, Termite Range Formation.|||19-MAR-20
11575|McNamara Group|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.|||
11575|McNamara Group|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Incorporates the Wide Supersequence and the Term Supersequence 1-3.|||Includes Lawn Hill Formation, Terminte Range Formation, Plain Creek Formation, Riversleigh Siltstone.||Grey to brown, siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite.|18-MAR-20
11575|McNamara Group|72526|5|Briefly described|p1, p4, p6, p8, p10, p85-86.|Calymmian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Shown p8 to be Statherian, but stated p1 to be late Paleoproterozoic to earliest Mesoproterozoic.Depositional ages from Page and Sweet, 1998; Page et al., 2000.|c. 1658 Ma to 1595 Ma dep. age from tuff (p4)||Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Termite Range, Lawn Hill, Drummond, Brumby, Plain Creek Formations; Shady Bore Quartzite, Riversleigh Siltstone, Bullrush Conglomerate.|Shown as partially overlying Sybella Granite and Gunpowder Creek Formation and shown as underlying South Nicholson Group.|Inlcudes quartzite and conglomerate.|
11575|McNamara Group|72527|4|Described|p1,p3, p5, p10, p12, p27, p87, p91, p98|Paleoproterozoic|Paleoproterozoic|See also p105, p112, p119-120, p132, p140, p147, p161, p193-196.|||Includes Widdallion Sandstone Member, Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Brumby Formation, Bullrush Conglomerate, Drummond Formation, Paradise Creek Formation.|Unconformably underlies the South Nicholson Group. Possible correlation with Benmara Group.|Includes friable brown to purple lithic and micaceous fine to coarse-grained sandstone and minor laminated siltstone and claystone. Quartzite with abundant pebble lags and gritty lenses, bedded polymict granule, pebble to cobble conglomerate.|
11575|McNamara Group|72889|6|Mentioned|p6 Fig.i.|||||||||
11575|McNamara Group|72912|4|Described|p5 Fig.3, p13-14, p17, p24-25.|Paleoproterozic|Paleoproterozic|Part of Isa Superbasin. Shown as being located in both Queensland and Northern Territory. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Has potential to host shale gas deposits. See also p32, p33, p35, p45-47.|||Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta, Termite Range, Lawn Hill, Drummond, Brumby, Plain Creek Formations; Shady Bore Quartzite, Riversleigh Siltstone, Bullrush Conglomerate.|Shown as partially underlying South Nicholson Group.|Mixed clastic sediments and carbonates.|
11575|McNamara Group|72913|5|Briefly described|p7, p9 Tb.1.|Paleoproterozoic|Paleoproterozoic|Shown as being in the Lawn Hill Platform and eastern part of the Isa Superbasin.|||Includes Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Lady Loretta Formation, Shady Bore Quartzite, Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation.|Shown as lateral equivalent to Fickling Group and underlying South Nicholson Group.|Include organic rich siltstone, dolomitic siltstone, sandstone, dolostone.|
11575|McNamara Group|72919|6|Mentioned|p3, p5, p25, p71, p98|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.|||Lawn Hill Formation, Plain Creek Formation, Shady Bore Quartzite, Brumby Formation, Drummond Formation, Bullrush Conglomerate|Unconformably underlain by Surprise Creek Formation. Unconformably overlain by Wangalinji Member (Playford Sandstone, Wild Cow Subgroup, South Nicholson Group). Equivalent to Benmara Group.||
11575|McNamara Group|72949|6|Mentioned|p35|Calymmian|Statherian|Mount Isa Inlier, Western Fold Belt.||||||
11575|McNamara Group|72967|6|Mentioned|p2, p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.|||Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Walford Dolostone*, Lady Loretta Formation|||
11575|McNamara Group|73042|6|Mentioned|p1, p3-4, p6, p11, p13|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region and Mount Isa Province.|||Riversleigh Siltstone, Lawn Hill Formation and more (see p4 Fig.1.2).|||
11575|McNamara Group|73083|6|Mentioned|p35, p72|Paleoproterozoic|Paleoproterozoic|||||||
11575|McNamara Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
11575|McNamara Group|73144|6|Mentioned|p8|Calymmian|Statherian|Isa Superbasin. [informal upper and lower are indicated in Fig.2]. Spans the Doom, Wide, Lawn, Term, River, Loretta, and Gun supersequences. Includes aquifers, partial aquifers, leaky aquitards and aquitards. Includes potential shale gas/oil plays and potential tight gas/oil.|||Lawn Hill Formation, Termite Range Formation, Riversleigh Siltstone, Lady Loretta Formation, Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation, and members therein|||14-OCT-22
11575|McNamara Group|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
11575|McNamara Group|73418|6|Mentioned|p4|||Mount Oxide Domain.|||||Carbonaceous metasedimentary rocks.|
11718|Merrimelia Formation|13497|3|Fully described|iv, v, vi, viii, x, xi|Asselian|Stephanian|Cooper Basin. Name is derived from the local aboriginal word Merrimelia (Martin 1967b). A type section in core is mentioned and a sedimentary facies log of this type core is given on p76. Outcrop characteristics discussed briefly. Deposited in a glacial environment. Has poor oil source quality and richness. See also xii, xiii, p47-p48, p54, p61, p64-p67, p69 fig 6.1, p70, p75-p84, p86-p89, p119, p122, p131, p132 tbl 8.1, p138, p139 fig 8.18, p141, p146, p152 fig 9.25, p153, p157-p159, p173, p184, p190, p216.||Gidgealpa Group||Interfingers with and is overlain by the Tirrawarra Sandstone. Unconformably overlain by the Patchawarra Formation.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|
11718|Merrimelia Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
11718|Merrimelia Formation|22527|6|Mentioned|p 3, Fig 3|||||||||
11718|Merrimelia Formation|22839|6|Mentioned|P33|||||||||
11718|Merrimelia Formation|22883|6|Mentioned|P29|||Overlying unit is Tirrawarra Sandstone||||||
11718|Merrimelia Formation|23154|5|Briefly described|Map Legend|Early Permian||Geological Province - Cooper Basin.  Of the Gidgealpa Group.  Max age ? Late Carboniferous.||||||06-NOV-06
11718|Merrimelia Formation|23155|4|Described|p14|Early Permian|Late Carboniferous|Unit forms the base of the Gidgealpa Group.  Sparse spore pollen assemblages suggest a Late Carboniferous to Early Permian age.  Overlying unit on STRZELECKI - Tirrawarra Sandstone.||||||
11718|Merrimelia Formation|23375|4|Described|Fig2 p265,285||Asselian|In the Cooper Basin.||||||06-NOV-06
11718|Merrimelia Formation|23818|5|Briefly described|p123 Fig.54, p128|Sakmarian|Sakmarian|Geological Province: Cooper Basin. Max. thickness: 1190 ft.||||||
11718|Merrimelia Formation|23830|5|Briefly described|Fig. 3a|Permian|Carboniferous|Geological Province: eastern Arckaringa Basin and Cooper Basin.||||||12-SEP-05
11718|Merrimelia Formation|23832|4|Described|p327|Permian|Permian|Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|24210|5|Briefly described|p133 Fig. 2|Late Carboniferous|Late Carboniferous|Of the Gidgealpa Group. Glacial deposits. Geological Province: Cooper Basin. See also p132.||||||14-APR-08
11718|Merrimelia Formation|24212|5|Briefly described|p67 Fig. 3p|Early Permian|Early Permian|Age: >290Ma.  Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
11718|Merrimelia Formation|29391|6|Mentioned|Table 5|||See p23.||||||22-AUG-18
11718|Merrimelia Formation|29393|6|Mentioned|Table 3|||Lower Permian.||||||
11718|Merrimelia Formation|29497|6|Mentioned|p31|||||||||
11718|Merrimelia Formation|29516|6|Mentioned|p25|||||||||
11718|Merrimelia Formation|30340|6|Mentioned|p2517|||Lithology||||||
11718|Merrimelia Formation|30341|5|Briefly described|p122|||Permian age.||||||06-NOV-06
11718|Merrimelia Formation|30540|6|Mentioned|Fig.6|||||||||
11718|Merrimelia Formation|30804|6|Mentioned|p10|||On Table 1.||||||
11718|Merrimelia Formation|30825|6|Mentioned|p37|||||||||
11718|Merrimelia Formation|30856|4|Described|Table 2|||Lower Permian age. See also p9.||||||06-NOV-06
11718|Merrimelia Formation|30857|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|30873|5|Briefly described|p15|||||||||
11718|Merrimelia Formation|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
11718|Merrimelia Formation|31145|5|Briefly described|Table 1|||Lower Permian||||||
11718|Merrimelia Formation|31250|6|Mentioned|p8|||Microflora||||||
11718|Merrimelia Formation|31431|5|Briefly described|Table 2|||L.Permian||||||
11718|Merrimelia Formation|31436|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|31591|6|Mentioned|p54|||See also p56, 57.||||||22-AUG-18
11718|Merrimelia Formation|31923|6|Mentioned|p12|||||||||
11718|Merrimelia Formation|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7||||||
11718|Merrimelia Formation|33067|4|Described|Table 1|Permian|Permian|Sandstone, siltstone, coal, conglomerate.||||||07-JUL-04
11718|Merrimelia Formation|33074|5|Briefly described|p260|||||||||
11718|Merrimelia Formation|33078|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|33079|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|33082|6|Mentioned|Map legend|Permian|Permian|||||||
11718|Merrimelia Formation|33089|5|Briefly described|Table 2|||Permian||||||
11718|Merrimelia Formation|33331|6|Mentioned|p38|||||||||
11718|Merrimelia Formation|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
11718|Merrimelia Formation|33523|6|Mentioned|p23|||||||||
11718|Merrimelia Formation|33827|6|Mentioned|Table 2|||||||||
11718|Merrimelia Formation|33844|6|Mentioned|p56|||Refers Martin (1967)||||||
11718|Merrimelia Formation|33936|6|Mentioned|Fig.3A|||||||||
11718|Merrimelia Formation|33971|6|Mentioned|p34|||Lithology similar to Crown Pt. Fm.||||||
11718|Merrimelia Formation|33976|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|33977|5|Briefly described|p7|||Strat. Refers Martin (1967).||||||
11718|Merrimelia Formation|33998|6|Mentioned|p28|||||||||
11718|Merrimelia Formation|34065|6|Mentioned|p9|||L.Perm.||||||
11718|Merrimelia Formation|34218|6|Mentioned|p9|||Lower Permian||||||
11718|Merrimelia Formation|34309|6|Mentioned|p42|||Permian||||||
11718|Merrimelia Formation|34415|6|Mentioned|p79|||Lower Permian. See also pp80,81,82 etc.||||||22-AUG-18
11718|Merrimelia Formation|34487|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
11718|Merrimelia Formation|34612|4|Described|p128|||Permian. Sub-surface only.||||||
11718|Merrimelia Formation|34839|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|35067|6|Mentioned|Fig.4|||||||||
11718|Merrimelia Formation|35068|6|Mentioned|p52|||See also Fig.3||||||
11718|Merrimelia Formation|35279|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
11718|Merrimelia Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
11718|Merrimelia Formation|35615|6|Mentioned|p1146|||||||||
11718|Merrimelia Formation|35845|4|Described|p23|||Lithology and depositional environments.||||||
11718|Merrimelia Formation|36099|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|36596|6|Mentioned|Text Fig.2|||||||||
11718|Merrimelia Formation|36910|6|Mentioned|p61|||||||||
11718|Merrimelia Formation|36917|6|Mentioned|Fig.1|||||||||
11718|Merrimelia Formation|37065|6|Mentioned|p32|||||||||
11718|Merrimelia Formation|37287|6|Mentioned|p36|||||||||
11718|Merrimelia Formation|37565|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|37855|6|Mentioned|p4|||See also Fig.2||||||
11718|Merrimelia Formation|37917|4|Described|p470|||||||||
11718|Merrimelia Formation|37926|6|Mentioned|p500|||||||||
11718|Merrimelia Formation|38068|5|Briefly described|p70|||||||||
11718|Merrimelia Formation|38226|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|38779|6|Mentioned|p7|||||||||
11718|Merrimelia Formation|38977|6|Mentioned|p1423|||||||||
11718|Merrimelia Formation|39254|4|Described|p45|||||||||
11718|Merrimelia Formation|39261|6|Mentioned|Fig. 9|||||||||
11718|Merrimelia Formation|39264|6|Mentioned|Fig. 13|||||||||
11718|Merrimelia Formation|39265|6|Mentioned|Fig. 3|||||||||
11718|Merrimelia Formation|39276|6|Mentioned|Fig. 2|||||||||
11718|Merrimelia Formation|39445|5|Briefly described|Table 7|||||||||
11718|Merrimelia Formation|39478|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|39494|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|39904|6|Mentioned|p14|||||||||
11718|Merrimelia Formation|40003|6|Mentioned|Fig.9|||||||||
11718|Merrimelia Formation|40030|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|40249|6|Mentioned|p45|||||||||
11718|Merrimelia Formation|40544|6|Mentioned|Fig.4|||||||||
11718|Merrimelia Formation|40637|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|40675|6|Mentioned|Table 12D|||||||||
11718|Merrimelia Formation|41097|6|Mentioned|p165|||||||||
11718|Merrimelia Formation|41099|6|Mentioned|p185|||||||||
11718|Merrimelia Formation|41131|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|41164|6|Mentioned|p422|||||||||
11718|Merrimelia Formation|41166|4|Described|p379|||||||||
11718|Merrimelia Formation|41183|6|Mentioned|Fig.3 p308|||||||||
11718|Merrimelia Formation|41198|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|41214|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|41247|6|Mentioned|Fig.5|||||||||
11718|Merrimelia Formation|41267|6|Mentioned|Fig.2|||||||||
11718|Merrimelia Formation|41288|6|Mentioned|Fig.12|||||||||
11718|Merrimelia Formation|41491|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|41595|6|Mentioned|Fig. 4|||||||||
11718|Merrimelia Formation|41689|6|Mentioned|Table 1|||||||||
11718|Merrimelia Formation|41707|6|Mentioned|Fig.8|||||||||
11718|Merrimelia Formation|42042|6|Mentioned|p244|||||||||
11718|Merrimelia Formation|42062|6|Mentioned|p26|||||||||
11718|Merrimelia Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||06-NOV-06
11718|Merrimelia Formation|42357|5|Briefly described|p4|||||||||
11718|Merrimelia Formation|42395|6|Mentioned|p79|||||||||
11718|Merrimelia Formation|42547|4|Described|p80|||||||||
11718|Merrimelia Formation|42746|5|Briefly described|p3, Fig.2 p4|||In the Cooper Basin.||||||06-NOV-06
11718|Merrimelia Formation|42966|6|Mentioned|p63|||||||||
11718|Merrimelia Formation|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
11718|Merrimelia Formation|43002|5|Briefly described|Fig.2,p135|||||||||
11718|Merrimelia Formation|43004|5|Briefly described|Table 1,p179|||||||||
11718|Merrimelia Formation|43052|5|Briefly described|Table 2.1|||||||||
11718|Merrimelia Formation|43105|5|Briefly described|p14|||||||||
11718|Merrimelia Formation|43218|6|Mentioned|p26|||Cooper Basin. Correlated with Urana Formation, Murray Basin.||||||
11718|Merrimelia Formation|43570|5|Briefly described|Fig.2,p535,541|Early Permian|Late Carboniferous|||||||
11718|Merrimelia Formation|43628|6|Mentioned|Fig.3||Early Permian|||||||
11718|Merrimelia Formation|43841|6|Mentioned|7|||In Cooper Basin||||||
11718|Merrimelia Formation|44020|14|Not recorded|p9,10,13,Tb.1,2||Early Permian|||||||
11718|Merrimelia Formation|44133|5|Briefly described|p65 Fig 8.4, 82|Permian|Carboniferous|Of the Gidgealpa Group. Geological Province: Cooper Basin. Thickness: >290m.||||||
11718|Merrimelia Formation|45104|6|Mentioned|p30|||||||||
11718|Merrimelia Formation|46849|6|Mentioned|Fig. 7|||||||||
11718|Merrimelia Formation|48995|6|Mentioned|Fig.3|||||||||
11718|Merrimelia Formation|60386|6|Mentioned|p296|Sakmarian|Asselian|Cooper Basin. Non-marine.||||||
11718|Merrimelia Formation|60717|5|Briefly described|p40, p41|Late Carboniferous|Late Carboniferous|Of the Gidgealpa Group. Overlain by Tirrawarra Sandstone. Thickness: 450m. Geological Province: Cooper Basin. Glacial, lacustrine, aeolian deposits. See also Figure 2.||||||14-APR-08
11718|Merrimelia Formation|61614|6|Mentioned|p290 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
11718|Merrimelia Formation|61615|5|Briefly described|p302, p303, p302 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin. Glacial deposits.||||||07-FEB-11
11718|Merrimelia Formation|61616|6|Mentioned|p330 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|61617|6|Mentioned|p343|Permian|Permian|Geological Province: Cooper Basin.||||||
11718|Merrimelia Formation|62046|5|Briefly described|p125 Fig. 2|Carboniferous|Carboniferous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
11718|Merrimelia Formation|62537|6|Mentioned|p191 Fig.2, p192 .|Early Permian|Late Carboniferous|Cooper Basin. The basal sediments of the Merrimelia Formation were deposited around 295-305 Ma and uncomformably overlie the Warburton Basin.||Unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone.||22-AUG-18
11718|Merrimelia Formation|62730|5|Briefly described|p352 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Cooper Basin.||||||14-APR-08
11718|Merrimelia Formation|63832|5|Briefly described|p131 Fig.2, p135|Cisuralian|Cisuralian|Cooper Basin. Is mentioned on p135 as the abbreviated [and mis-spelt] Tirrawarra-Merimelia Formations. Thick succession of continental proglacial and possibly subglacial facies.||||Is overlain by and interfingers with Tirrawarra Sandstone.|Continental proglacial and possibly subglacial facies.|13-DEC-17
11718|Merrimelia Formation|63978|2|Defined|p8, p9-10, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Group. Intertongues with Tirrawarra Sandstone (mapped tog.as one 'unit'  in Fig. 13). Max.thick: 84m. Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone + shale, commonly green-grey. Geol.prov: base of Cooper Basin.||||||07-FEB-11
11718|Merrimelia Formation|64048|5|Briefly described|p64 Tb. 2|||Geological Province: Cooper Basin. Oil reservoir at Malgoona.||||||07-FEB-11
11718|Merrimelia Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Early Permian|Late Carboniferous|Cooper Basin.||||Underlies Tirrawarra Sandstone and Patchawarra Formation.||11-DEC-15
11718|Merrimelia Formation|64631|5|Briefly described|p49.|Sakmarian|Asselian|Cooper Basin. Contains thick successions of continental proglacial facies. See also p44. Some biostratigraphic age control. Shown with time transgressive top boundary.||||Overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hydrocarbon reservoirs are thought to have been charged from Patchawarra Formation.||||Is overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|65489|5|Briefly described|p16, p48-49, p55, p96, p131-132, p143|Asselian|Late Carboniferous|Cooper Basin. 450m thick. Oil reservoir accounting for 1% of the Basin's production.||Basal unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone and Patchawarra Formation. Equivalent to Crown Point Formation.|Terminoglacial and glaciofluvial systems including aeolianite.|
11718|Merrimelia Formation|65925|5|Briefly described|Appendix 2.||||||||Conglomerates, sandstone, glacigene lacustrine rhythmites.|
11718|Merrimelia Formation|67402|5|Briefly described|p90, p90 fig CPR4|||Deposited in glacio-fluvial environments. See also p91 tbl CPR1, p91, p92, p94, p101, p101 tbl CPR2.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone and Patchawarra Formation.|Glacial conglomerates, diamictites, sandstone, siltstone and shale.|
11718|Merrimelia Formation|67561|6|Mentioned|p67|||||||||
11718|Merrimelia Formation|68068|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Cooper Basin (subsurface only). Age from sparse spore-pollen assemblage. Fluvioglacial outwash, lacustrine (shallow to relatively deep water), subaerial and subaqueous tillites.||Basal unit in Gidgealpa Group.||Is conformably overlain by Tirrawarra Formation.|Buff-white, fine-grained sandstone, rippled, soft-sediment deformation; massive to crudely-bedded conglomerate; poorly-sorted diamictite, matrix-supported, dropstones; dark grey claystone and siltstone, flat-laminated or with sandstone interbeds.|
11718|Merrimelia Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian||Cooper Basin. Gravestock et al. (1995) included this formation in the Gidgealpa Group. ~ 80 m thick. A Cisuralian age is suggested based on a basement granite (298 +/- 4 Ma) in the Nappamerri Trough and assignment of palynofloras.||Of the Gidgealpa Group.||Interdigitated with the overlying Tirrawarra Sandstone. Unconformably overlain by the Patchawarra Formation.|Includes proglacial fluvial outwash deposits, termino-glacial fluvial deposits and varvites to delta front debris flows and deepwater lacustrine deposits.|17-JUL-14
11718|Merrimelia Formation|69023|4|Described|p79-83, p163, p191-192|Permian|Late Carboniferous|Cooper Basin. Defined by Martin (1967). Was excluded from the original Gidgealpa Group (Martin, 1967; Gatehouse, 1972) but later included (Callen et al.,1994; Gravestock et al., 1995, and this study). Oil and gas reserves. Fluvio-glacial. Conglomerate clasts mainly from Mooracoochie Volcanics and, locally, reworked glauconite from Pando Formation. Very uneven distribution. 175 to >512m thick. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies Dullingari Group. Is overlain by Patchawarra Formation and Tirrawarra Sandstone.|Massive to crudely-bedded conglomerate; fine- to medium-grained sandstone, massive, or flat and planar cross-bedded; subordinate thin, grey-brown siltstone beds and laminations which can be pyritic and carbonaceous; minor shale, coal seams.|
11718|Merrimelia Formation|69454|5|Briefly described|p38:4|Asselian|Asselian|Cooper Basin.||Gidgealpa Group.||Correlated with Crown Point Formation (Pedirka Basin).||12-JUL-16
11718|Merrimelia Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Tirrawarra Sandstone||
11718|Merrimelia Formation|69797|5|Briefly described|p17 Fig.2|Late Carbonfierous|Late Carbonfierous|Age: Stephanian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
11718|Merrimelia Formation|69946|5|Briefly described|p3, p9, p36, p45, p54|Asselian|Late Carboniferous|Southern Cooper Basin. Glaciofluvial unit deposited unconformably on deformed Warburton Basin strata and exposed granites.||Basal unit in Gidgealpa Group.||Is overlain by Tirrawarra Sandstone conformably and Patchawarra Formation unconformably. Equivalent to Boorthanna Formation (Arckaringa Basin).||
11718|Merrimelia Formation|69947|5|Briefly described|p13 Fig.7.2, p16-17 Figs.7.5-6|Permian|Late Carboniferous|See also p21 Fig.7.10. Cooper Basin.||Gidgealpa Group.||||
11718|Merrimelia Formation|69982|5|Briefly described|p13, p24, p44, Appendix 1|||Cooper Basin. Moolalla 1 gas field, discovered in this unit (Baily, 1990), was later assigned to the Pando Formation in the underlying Warburton Basin. Brief thin section descriptions.||Unit in the Gidgealpa Group.|||Quartz is coarse-grained; muscovite is not altered to chlorite.|
11718|Merrimelia Formation|70317|6|Mentioned|p33|Late Carboniferous|Late Carboniferous|Cooper Basin.||Gidgealpa Group.||Is overlain, locally unconformably, by Tirrawarra Sandstone.||
11718|Merrimelia Formation|70823|4|Described|iv, p25-p27, 51-53|Asselian|Gzhelian|Cooper Basin. Up to 620m thick. Deposited in a terminoglacial, proglacial, glaciolacustrine or aeolian environment. Age debated.Overlies granodiorites with minimum emplacment age of 307 Ma.Palynofloras consistent with APP1.21, 1.22 ie up to top Asselian. Hosts a commercial reservoir that is briefly discussed. See also p36, p40-p41, p51-p53, p78-p80, p82.||Gidgealpa Group||Overlain by and interfingers with the Tirrawarra Sandstone. Underlain by Big Lake Suite granodiorites.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|22-AUG-18
11718|Merrimelia Formation|70824|4|Described|p7-p9, p38-p44, p122|Asselian|Gzhelian|Cooper Basin. Up to 620m thick. Deposited in terminoglacial, proglacial, glaciolacustrine or aeolian environments. Outcrop and areal extent briefly discussed.||||Overlain by the Tirrawarra Sandstone.|Conglomerate, diamictite, sandstone, conglomeratic mudstone, siltstone and shale.|
11718|Merrimelia Formation|70946|5|Briefly described|p1089|Carboniferous|Carboniferous|Cooper Basin. Deposited in a terminoglacial, proglacial, glaciolacustrine and aeolian environments.||Gidgealpa Group.||||08-OCT-18
11718|Merrimelia Formation|71265|5|Briefly described|p589|Asselian|Gzhelian|Cooper Basin.||Gidgealpa Group.||Is overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36, Ch5 p45|Asselian|Stephanian|Cooper Basin. Deposited in a glaciofluvial, proglacial, aeolian or glaciolacustrine envrionment. Palynological zone is given in fig 5.3 Ch5 p36. Thermal history briefly discussed in Ch9. See also Ch5 p54, Ch7 p13, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p14, Ch10 p19-p20.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone.||
11718|Merrimelia Formation|71701|5|Briefly described|p155|Asselian|Kasimovian|Cooper Basin.||Gidgealpa Group||Overlain by the Tirrawarra Sandstone.||
11718|Merrimelia Formation|72478|6|Mentioned|Fig. 7 p70|||||||||
11718|Merrimelia Formation|72497|5|Briefly described|p17 Fig.11, p13.|Early Permian|Late Carboniferous|Cooper Basin. Described as glaciolacustrine, glaciofluvial, tillites environment.||||Underlies Tirrawarra Sandstone with diachronous contact?||
11718|Merrimelia Formation|73167|5|Briefly described|p662, p664, p672|late Carboniferous|late Carboniferous|Cooper Basin. Deposited on regional unconformity above the Warburton Basin. Onlaps onto the Gidgealpa-Merrimelia-Innamincka and Murteree-Nappacoongee ridges. Shown as lower Permian in Fig. 2, p664 and spelt Merrimellia Formation. Contains oil and gas.|||||Glacial sediments.|
11718|Merrimelia Formation|73251|6|Mentioned|p62|Late Carboniferous|Late Carboniferous|Cooper Basin. Terminoglacial, proglacial, glaciolacustrine, and aeolian depositional environments. Contains[?] gas.||Gidgealpa Group||Overlain by Tirrawarra Sandstone.||
11718|Merrimelia Formation|73343|6|Mentioned|p338|Late Carboniferous|Late Carboniferous||||||Glacial sediments.|
11718|Merrimelia Formation|73479|5|Briefly described|p157, p166, p176|Permian|Permian|Base of the Cooper Basin. Glacial unit.|ca 290 Ma|||Underlies Tirrawarra Formation||
11718|Merrimelia Formation|73495|5|Briefly described|p499, p503-504|||Cooper Basin. Deposited in a complex array of glaciolacustrine, terminoglacial and proglacial environments.||Gidgealpa Group||Overlain by and interfingering with Tirrawarra Sandstone. Unconformably overlain by Patchawarra Formation.|Diamictites, sandstones, conglomeratic mudstones, siltstones and shales.|
11776|Mick Creek Sandstone Member|22461|5|Briefly described|Fig 2 p466|||Parent: Marimo Slate||||||
11776|Mick Creek Sandstone Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
11776|Mick Creek Sandstone Member|30531|2|Defined|p22|Precambrian|Precambrian|||||||
11776|Mick Creek Sandstone Member|39496|6|Mentioned|p14|||||||||
11776|Mick Creek Sandstone Member|41791|6|Mentioned|p255|||||||||
11776|Mick Creek Sandstone Member|45166|5|Briefly described|p24|||||||||
11836|Milkman Creek Member|30451|5|Briefly described|p16|||See also Fig.2||||||
11836|Milkman Creek Member|31999|5|Briefly described|p149|||Table 1||||||
11836|Milkman Creek Member|32140|6|Mentioned|p9|||Mb. Dawes Range Fm. Dev.||||||
11836|Milkman Creek Member|32865|6|Mentioned|p479|||Davies Range Fm. Fauna||||||
11836|Milkman Creek Member|44379|2|Defined|p3-6,Tb.1,3,map||Late Devonian|Unit of Dawes Range Formation.||||||
11840|Millaroo Granite|22847|3|Fully described|p 42|Ordovician|Early Ordovician|||||||
11840|Millaroo Granite|23084|4|Described|p675|Ordovician|Ordovician|||||||
11840|Millaroo Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
11840|Millaroo Granite|23504|5|Briefly described|Map Legend||Ordovician|||||||
11840|Millaroo Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 101. I-Type.||||||
11840|Millaroo Granite|30148|2|Defined|p16|Early Devonian|Late Silurian|Middle Ordovician & Upper Silurian or Lower Devonian||||||
11840|Millaroo Granite|30149|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician and Upper Silurian or?Lower Devonian||||||
11840|Millaroo Granite|30151|4|Described|Table 1|||Ravenswood Granodiorite Complex.||||||
11840|Millaroo Granite|31813|5|Briefly described|Table 2|||||||||
11840|Millaroo Granite|34409|6|Mentioned|Map legend|Early Devonian|Late Silurian|Middle Ordovician, Upper Silurian, Lower Devonian||||||
11840|Millaroo Granite|39686|6|Mentioned|p75|||||||||
11840|Millaroo Granite|41668|6|Mentioned|p12|||See also Table 2.2||||||
11840|Millaroo Granite|42245|5|Briefly described|p32|||||||||
11840|Millaroo Granite|43093|4|Described|Appendix 1|||Rb-Sr age of 470+/-30Ma.||||||
11840|Millaroo Granite|43259|4|Described|Appendix 1,p22.||Ordovician|||||||
11840|Millaroo Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
11840|Millaroo Granite|43936|5|Briefly described|Map Legend||Ordovician|||||||
11840|Millaroo Granite|45151|6|Mentioned|p29|||||||||
11840|Millaroo Granite|48914|2|Defined|p83|Early Devonian|Late Silurian|Middle Ordovician & Upper Silurian or Lower Devonian||||||
11840|Millaroo Granite|62079|5|Briefly described|p50-51|Ordovician|Ordovician|Hosts Mount Wright gold-mineralised breccia pipes: discussed in some detail. Is cut by a rhyolite dyke dated 304 Ma.|>304 Ma.||||Variable pink, fine- to coarse-grained biotite granite with localised zones and miarolitic cavities.|
11895|Miners Gap Granite|22847|3|Fully described|p 59|Early Permian|Carboniferous|||||||
11895|Miners Gap Granite|23422|5|Briefly described|p218 Table 6.12|||Of Leichhardt Suite.||||||
11895|Miners Gap Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
11895|Miners Gap Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 113. ?I-Type.||||||
11895|Miners Gap Granite|42245|2|Defined|p41|Permian||Reserved as Miners Gap Adamellite||||||
11895|Miners Gap Granite|43093|4|Described|Appendix 1|Early Permian|Carboniferous|Middle Carboniferous to Early Permian.||||||
11895|Miners Gap Granite|43259|4|Described|Appendix 1,p23.|Permian|Carboniferous|Carboniferous-Permian?.||||||
11895|Miners Gap Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Suite.||||
11899|Minerva Hills Volcanics|22993|5|Briefly described|p330 Table 1|Tertiary|Tertiary|||||||
11899|Minerva Hills Volcanics|34390|4|Described|Table 3|||Upper Oligocene||||||
11899|Minerva Hills Volcanics|34392|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11899|Minerva Hills Volcanics|34408|6|Mentioned|p185|||On Table||||||
11899|Minerva Hills Volcanics|37749|6|Mentioned|p186|||||||||
11899|Minerva Hills Volcanics|39445|5|Briefly described|Table 14|||||||||
11899|Minerva Hills Volcanics|41246|6|Mentioned|Map legend|Tertiary||||||||
11899|Minerva Hills Volcanics|41949|6|Mentioned|p117|||||||||
11899|Minerva Hills Volcanics|42614|5|Briefly described|p14|||||||||
11899|Minerva Hills Volcanics|43994|14|Not recorded|Map Legend|||||||||
11899|Minerva Hills Volcanics|43998|4|Described|p15,16,map||Tertiary|26+/-2Ma||||||
11899|Minerva Hills Volcanics|44337|5|Briefly described|Map Legend||Tertiary|Lithology.||||||
11899|Minerva Hills Volcanics|45071|3|Fully described|Table 15|||See also P88. 28 to 24 m.y.||||||
11899|Minerva Hills Volcanics|48845|2|Defined|p1,38-44,51,53,map,||Tertiary|Fig.19.||||||
11899|Minerva Hills Volcanics|61155|5|Briefly described|p20|Late Oligocene|Early Oligocene|In the Rockhampton-Gladstone area.||||||
11899|Minerva Hills Volcanics|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran, Gin Gin and Mount Runsome Basalts; Main Range, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
11899|Minerva Hills Volcanics|69599|5|Briefly described|p632 Fig.8.33, p636|||Sutherland et al. (1989). Constitutes the central zone of the Springsure central volcano. Forms silicic plugs and flows. 87Sr/86Sr isotopic values v. differentiation index diagram and comment. Appears as Minerva Volcanics on p632 Fig.8.33. Geochronology by Ewart (1982) and Webb and McDougall (1967) respectively.|28.6 +/- 1.8 Ma; 26.3 Ma.|||||
11899|Minerva Hills Volcanics|73450|4|Described|p4, p81-83|Rupelian|Rupelian|Crops out in the area north of Springsure; consists of a central felsic volcano and an apron of basaltic lavas forming plains and mesas. Forms protrusions, dykes and flows as radiating dyke complexes with auto-brecciated margins, and arcuate, domal and concentric intrusions. Emplaced during the second (middle) phase of volcanism associated with the Springsure central volcano. Yielded a sanidine Ar-Ar age of 28.1 +/- 0.3 Ma (Cohen et al., 2013) and a variety of K-Ar ages ranging from 26.3 Ma to 28.6 +/- 1.8 Ma. Interpreted to have been derived via fractional crystallisation from a basaltic/hawiitic parent (Ewart, 1982).|28.1 +/- 0.3 Ma Ar-Ar||||Trachyte, trachyrhyolite, comendite, quartz trachyte, and a variety of volcaniclastic rocks including pyroclastic deposits and autobreccias.|
11912|Mingoom Granite|23422|5|Briefly described|p183, p218 Table 6.12|Early Permian|Early Permian|Of Leichhardt Supersuite.||||||19-OCT-12
11912|Mingoom Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
11912|Mingoom Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 172. Assumed to be I-Type.||||||
11912|Mingoom Granite|42689|5|Briefly described|map legend|Early Permian|Carboniferous|||||||
11912|Mingoom Granite|43095|2|Defined|p78|Early Permian|Late Carboniferous|||||||
11912|Mingoom Granite|43259|4|Described|Appendix 1,p27.|Early Permian|Late Carboniferous|||||||
11912|Mingoom Granite|43589|2|Defined|p24|Early Permian|Early Permian|Intrudes Tareela and Saint Giles Volcanics and the Speed Creek Granite.||||||23-APR-08
11912|Mingoom Granite|68419|5|Briefly described|Map Legend|Permian|Permian|Of the Kennedy Province. Shown as Early Permian age.|||||Pink, mainly medium-grained, equigranular biotite granite.|
11912|Mingoom Granite|68420|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Kennedy Province.|||||Pink, mainly medium-grained, equigranular biotite granite.|
11912|Mingoom Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|||Hornblende-biotite and biotite granite and granodiorite.|
11923|Minmi Member|23982|5|Briefly described|p58 Fig.18|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|24092|5|Briefly described|p8 Fig.3|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|30020|6|Mentioned|p30|||||||||
11923|Minmi Member|30021|6|Mentioned|p87|||||||||
11923|Minmi Member|30022|6|Mentioned|p28|||||||||
11923|Minmi Member|30024|6|Mentioned|p336|||||||||
11923|Minmi Member|30446|6|Mentioned|p39|||||||||
11923|Minmi Member|30691|5|Briefly described|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30696|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30702|6|Mentioned|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30771|6|Mentioned|p4|||Cretaceous.Member of Hackdown Formation||||||
11923|Minmi Member|31116|4|Described|p41|||See also p42.||||||08-MAR-19
11923|Minmi Member|31208|6|Mentioned|Table 1|||||||||
11923|Minmi Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|32314|6|Mentioned|Fig. 4|||||||||
11923|Minmi Member|32796|6|Mentioned|p302|||||||||
11923|Minmi Member|34543|6|Mentioned|p98|||||||||
11923|Minmi Member|34613|6|Mentioned|p15|||||||||
11923|Minmi Member|34619|6|Mentioned|p.160, Pl.22||Adelaidean|||||||
11923|Minmi Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
11923|Minmi Member|36357|5|Briefly described|p77|||||||||
11923|Minmi Member|36552|6|Mentioned|p59|||||||||
11923|Minmi Member|36571|6|Mentioned|Table 4|||||||||
11923|Minmi Member|36574|6|Mentioned|p602|||||||||
11923|Minmi Member|37995|6|Mentioned|p66|||||||||
11923|Minmi Member|38373|6|Mentioned|p621|||||||||
11923|Minmi Member|38374|6|Mentioned|p605|||||||||
11923|Minmi Member|39211|5|Briefly described|p31|||||||||
11923|Minmi Member|39212|4|Described|p40|||Excursion site. See also p18.||||||08-MAR-19
11923|Minmi Member|39216|6|Mentioned|p55|||Fauna||||||
11923|Minmi Member|40541|4|Described|p111|||||||||
11923|Minmi Member|40666|4|Described|p358|||||||||
11923|Minmi Member|41057|6|Mentioned|p61|||||||||
11923|Minmi Member|41064|6|Mentioned|p60|||||||||
11923|Minmi Member|41266|6|Mentioned|Fig.3|||||||||
11923|Minmi Member|41427|6|Mentioned|p84|||||||||
11923|Minmi Member|42494|5|Briefly described|Table 1 P24|||||||||
11923|Minmi Member|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
11923|Minmi Member|44021|14|Not recorded|p232(Fig.1)|||||||||
11923|Minmi Member|44031|14|Not recorded|p11||Early Cretaceous|||||||
11923|Minmi Member|44082|6|Mentioned|p8,10,Tb.p34|||Part of Blythesdale Group. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
11923|Minmi Member|44376|4|Described|p1-9,11-8,20-3,25,29|||Fossils.||||||
11923|Minmi Member|44377|2|Defined|p1,2,10,13,map||Aptian|Top-most member of Blythesdale Formation. marine Aptian, mainly "calcareous and glauconitic protoquartzites", probably "near-shore facies equivalents of sediments in the lower part of the Roma Formation."||||||
11923|Minmi Member|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965.||||||
11923|Minmi Member|45110|3|Fully described|p112|||See also p10. Of Bungil Formation.||||||08-MAR-19
11923|Minmi Member|45132|6|Mentioned|Table 2|||||||||
11923|Minmi Member|46791|6|Mentioned|Table 1|||||||||
11923|Minmi Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
11923|Minmi Member|46984|6|Mentioned|Table 1|||||||||
11923|Minmi Member|48919|4|Described|Table 5|||||||||
11923|Minmi Member|48920|6|Mentioned|p59|||See also P73. Member of Blythesdale Formation.||||||
11923|Minmi Member|49010|6|Mentioned|Fig.4|||Surat Basin||||||
11923|Minmi Member|49011|6|Mentioned|Fig.3|||Surat Basin||||||
11923|Minmi Member|64856|4|Described|p98,99|early Aptian|early Aptian|Of Day (1964). Originally included in Blythesdale Formation, now in Bungil Formation. Contains early Aptian dinoflagellate assemblages.|| ||||31-JAN-13
11923|Minmi Member|65384|5|Briefly described|S116, S117, S118|||Probably Aptian.Of Bungil Formation, Surat Basin.||||||
11923|Minmi Member|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Bungil Formation.||Overlies Nullawurt Sandstone Member.||
11923|Minmi Member|66623|6|Mentioned|p449.|Early Cretaceous|Early Cretaceous|Contains various bivalve species which occur also in the Milparinka-Tibooburra district (Rolling Downs Group).||||||
11923|Minmi Member|69594|5|Briefly described|p538|Aptian|Aptian|Northern Surat Basin. Previously included by Day (1964) in his Blythesdale Formation. The type area is near Bungil Creek at Minmi Crossing. Contains a sproradic but diverse marine fauna dominated by molluscs, and the dinosaur Minmi paravertebra. Marine and brackish water environment.||Bungil Formation.|||Calcareous and glauconitic sandstones, silty shales and siltstones and minor intraformational conglomerates.|
11923|Minmi Member|70821|5|Briefly described|p80|||Surat Basin.||Bungil Formation.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla Formation).||
11923|Minmi Member|71601|6|Mentioned|p121|Aptian|Aptian|||Bungil Formation||||
11923|Minmi Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||Bungil FZ.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla FZ).||
11926|Minnages Mountain Granophyre|40896|5|Briefly described|p53|||||||||
11926|Minnages Mountain Granophyre|44778|14|Not recorded|p128,131-133,135|||(Post Triassic - pre Eocene-Oligocene)||||||
11926|Minnages Mountain Granophyre|45003|14|Not recorded|p59|||||||||
11980|Mitchell River Volcanics|23420|4|Described|p 146 table 4.5 + p 131||Permian|A-type affinities||||||26-APR-13
11980|Mitchell River Volcanics|23422|5|Briefly described|Plate 7.3|Late Permian|Late Permian|||||||
11980|Mitchell River Volcanics|23423|5|Briefly described|p265|||||||||
11980|Mitchell River Volcanics|23430|5|Briefly described|p489, p514.|||||||||
11980|Mitchell River Volcanics|23496|5|Briefly described|Table 3, p47|Late Permian|Late Permian|||||||
11980|Mitchell River Volcanics|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V86. I-Type.||||||
11980|Mitchell River Volcanics|23616|6|Mentioned|p83|||||||||
11980|Mitchell River Volcanics|23713|3|Fully described|p25-26||Late Permian|Previously included with Nychum Volcanic. Age: 274+/-5 Ma (K-Ar isotope).  Dargalong Province. Max. thickness <600 m.||||||
11980|Mitchell River Volcanics|30914|6|Mentioned|Map legend|Permian|Permian|||||||
11980|Mitchell River Volcanics|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
11980|Mitchell River Volcanics|39252|6|Mentioned|Fig. 15|||||||||
11980|Mitchell River Volcanics|39445|5|Briefly described|Table 8|||||||||
11980|Mitchell River Volcanics|42500|5|Briefly described|Fig. 3 (enclosure)|||Permian||||||
11980|Mitchell River Volcanics|42620|2|Defined|p165|Late Permian||K-Ar age 274+/-5Ma ie late Early Permian||||||
11980|Mitchell River Volcanics|43013|6|Mentioned|p242|||||||||
11980|Mitchell River Volcanics|43060|5|Briefly described|p116|||||||||
11980|Mitchell River Volcanics|43083|4|Described|p96|||Formerly included together with Nychum Volcanics. Age: 279+/-5 Ma (K-Ar). Diverse lithology of amygdaloidal to massive andesitic and dacitic/rhyodacitic lava flows, rhyolitic ignimbrite, minor felsic airfall and tuffaceous epiclastic sediments, and rare b||||||17-JUN-09
11980|Mitchell River Volcanics|43254|5|Briefly described|map legend||Late Permian|||||||
11980|Mitchell River Volcanics|43259|4|Described|Appendix 1,p8.||Permian|Age of 274+/-5 Ma. Age Early to Middle Permian.||||||
11980|Mitchell River Volcanics|43285|5|Briefly described|Map Legend||Late Permian|||||||
11980|Mitchell River Volcanics|43287|5|Briefly described|Map Legend||Late Permian|||||||
11980|Mitchell River Volcanics|43625|4|Described|p42|||Age: 274+/- Ma||||||
11980|Mitchell River Volcanics|60357|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Kennedy Province.||||||
11980|Mitchell River Volcanics|60425|6|Mentioned|p39|||Correlates with Little River Coal Measures. Fossil plant-bearing rocks.||||||07-FEB-11
11980|Mitchell River Volcanics|63154|5|Briefly described|p285 Fig. 5|Late Permian|Late Permian|Geological province: Coen Inlier.||||||
11980|Mitchell River Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek, Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork and Nychum Volcanics; the Little River Coal Measures, and the Normanby Formation, are all mapped under the symbol, Pvk.||||||
11980|Mitchell River Volcanics|69591|6|Mentioned|p102|Permian|Permian|||||||
11980|Mitchell River Volcanics|69593|6|Mentioned|p483, p485|||Herberton and/or Tate Subprovinces, Kennedy Igneous Association.||||||
11983|Mitchiebo Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
11983|Mitchiebo Volcanics|38237|6|Mentioned|Fig.3|||||||||
11983|Mitchiebo Volcanics|39338|5|Briefly described|p352|||||||||
11983|Mitchiebo Volcanics|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of Carrara Range Gp.  Strongly altered vesicular and amygdaloidal basalt or trachyte; feldspathic and lithic sandstone; minor micaceous siltstone and shale.  Conformably overlies Don Creek Sst; unconformably overlain by Top Rocky Rhyolite, Musselbrook Fm.||||||10-JAN-05
11983|Mitchiebo Volcanics|39497|4|Described|p7|||||||||
11983|Mitchiebo Volcanics|39925|6|Mentioned|p337|||||||||
11983|Mitchiebo Volcanics|40811|6|Mentioned|p318|||||||||
11983|Mitchiebo Volcanics|45166|5|Briefly described|p27|||||||||
11983|Mitchiebo Volcanics|49018|2|Defined|p4|Carpentarian|Carpentarian|||||||
11983|Mitchiebo Volcanics|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. Weathered or altered, massive to vesicular or microvesicular basalt and microdolerite; minor sandstone, mudstone and peperite.||||||
11983|Mitchiebo Volcanics|63866|5|Briefly described|p57|||Carrara Range, Leichhardt Superbasin.||||Overlain by the Top Rocky Rhyolite. Possibly equivalent to the Eastern Creek Volcanics.||
11983|Mitchiebo Volcanics|65337|4|Described|p6 Fig.3, p10 Table 3, p13.|||500-1000 m thick subaerial lava flows and shallow invasive flows. The upper sandstone part (Sweet 1984) is defined in this study as the new unit, Gator Sandstone. Resembles Seigal Volcanics, Eastern Creek Volcanics and Buddawadda Basalt. Highly magnetic.||Unit in Carrara Range Group.||Overlies Don Creek Sandstone. Is overlain by Gator Sandstone.|Weathered and/or altered, massive to vesicular or microvesicular basalt and microdolerite; lesser sandstone, mudstone and peperite.|
11983|Mitchiebo Volcanics|69433|4|Described|p18:2, 5-7|Statherian|Statherian|Southern succession, Lawn Hill Platform. 500-1000m thick. Is lithologically and geochemically indistinguishable from Seigal Volcanics (McArthur Basin). Is correlated with Seigal and Eastern Creek Volcanics and Buddawadda Basalt.||Carrara Range Group.||Conformably overlies Don Creek Sandstone. Is overlain by Gator Sandstone conformably, or Surprise Creek Formation and (locally) Top Rocky Rhyolite unconformably.|Weathered and/or altered, massive to vesicular or microvesicular basalt and microdolerite, with interbeds of sandstone, mudstone and peperite.|12-JUL-16
11983|Mitchiebo Volcanics|69673|4|Described|p52 fig 42,|||Up to 1km thick.||Carrara Range Group|||Basalt and microdolerite with interbeds of sandstone, mudstone and peperite.|
11983|Mitchiebo Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.||
11983|Mitchiebo Volcanics|72527|6|Mentioned|p7 Fig.1.4, p120, p169.|Paleoproterozoic|Paleoproterozoic|Rawlings et al. (2008) subdivided this unit creating the newly named Gator Sandstone at the top.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.|Rhyolite clasts locally comprise as much as 10-15 percent of the total clast population; the remaining clasts are dominated by sandstone, siltstone, mudstone, layered chert, milky vein quartz and possibly small fragments of mafic volcanics.|
11983|Mitchiebo Volcanics|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the East part of the South Nicholson Basin and Lawn Hill Platform.||Carrara Range Group||Overlies Don Creek Sandstone and underlies Gator Sandstone.||
11983|Mitchiebo Volcanics|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Underlain by Don Creek Sandstone. Overlain by Gator Sandstone.||
11983|Mitchiebo Volcanics|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
11984|Mithaka Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Siltstone, sandstone; mudstone.  Overlain by Cravens Peak beds.||||||21-JUN-04
11984|Mithaka Formation|8217|5|Briefly described|Map Legend|Ordovician|Ordovician|Siltstone, sandstone.||||||
11984|Mithaka Formation|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Mudstone, quartzose sandstone.||||||19-AUG-04
11984|Mithaka Formation|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Late Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
11984|Mithaka Formation|13995|6|Mentioned|p101|Middle Ordovician|Middle Ordovician|Georgina Basin.||||||
11984|Mithaka Formation|22646|6|Mentioned|Fig 5 on p 105|Late Ordovician|Early Ordovician|In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
11984|Mithaka Formation|23858|5|Briefly described|p924 Fig 8|Ordovician||||||||
11984|Mithaka Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 120m.||||||
11984|Mithaka Formation|24442|6|Mentioned|p49|||On TOBERMORY sheet.||||||
11984|Mithaka Formation|33111|4|Described|p38|||Mention Fig.9||||||
11984|Mithaka Formation|33738|6|Mentioned|p54|||||||||
11984|Mithaka Formation|34454|5|Briefly described|Table 2|||M.Ordovician||||||
11984|Mithaka Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||06-NOV-06
11984|Mithaka Formation|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
11984|Mithaka Formation|35139|4|Described|Table.2|||||||||
11984|Mithaka Formation|35146|6|Mentioned|p470|||||||||
11984|Mithaka Formation|36234|3|Fully described|p174|||||||||
11984|Mithaka Formation|36243|6|Mentioned|Table 1A|||||||||
11984|Mithaka Formation|36580|6|Mentioned|p469|||See also Fig.1.||||||06-NOV-06
11984|Mithaka Formation|37572|4|Described|p164|||See also Fig.8.||||||06-NOV-06
11984|Mithaka Formation|38832|6|Mentioned|p157|||||||||
11984|Mithaka Formation|39445|5|Briefly described|Table 4|||||||||
11984|Mithaka Formation|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
11984|Mithaka Formation|39943|6|Mentioned|Table 2A|||||||||
11984|Mithaka Formation|40136|5|Briefly described|p31|||||||||
11984|Mithaka Formation|40810|5|Briefly described|p15|||||||||
11984|Mithaka Formation|40906|6|Mentioned|Fig.11|||||||||
11984|Mithaka Formation|41524|6|Mentioned|Fig.3|||||||||
11984|Mithaka Formation|42059|6|Mentioned|Fig.2 P131|||||||||
11984|Mithaka Formation|42060|6|Mentioned|Fig.5 P140|||||||||
11984|Mithaka Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
11984|Mithaka Formation|43236|6|Mentioned|p14||Ordovician|In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|43803|6|Mentioned|Fig.5,p71|||||||||
11984|Mithaka Formation|44308|14|Not recorded|p10,14,Tb.1||Early Ordovician|Of Toko Group.||||||
11984|Mithaka Formation|44309|2|Defined|Tb.1,p7,12-3,17,19,||Ordovician|Unit of Toko Group. Overlies Carlo Sandstone. Map.||||||
11984|Mithaka Formation|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
11984|Mithaka Formation|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
11984|Mithaka Formation|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
11984|Mithaka Formation|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||11-FEB-09
11984|Mithaka Formation|44469|2|Defined|p.10, Tb.I|Middle Ordovician|Middle Ordovician|(F53-12). Conformably overlies Carlo Sandstone. Of the Toko Group.  Fossils. See also p.16.||||||09-FEB-17
11984|Mithaka Formation|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
11984|Mithaka Formation|44848|14|Not recorded|p111|||||||||
11984|Mithaka Formation|44852|14|Not recorded|p71||Ordovician|||||||
11984|Mithaka Formation|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
11984|Mithaka Formation|45052|3|Fully described|p130|||M.Ord. See also p38.||||||06-NOV-06
11984|Mithaka Formation|45118|6|Mentioned|p3|||||||||
11984|Mithaka Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||06-NOV-06
11984|Mithaka Formation|45155|6|Mentioned|Fig.8|||||||||
11984|Mithaka Formation|46841|6|Mentioned|p97|||||||||
11984|Mithaka Formation|46940|4|Described|p57|||||||||
11984|Mithaka Formation|46956|6|Mentioned|p160|||||||||
11984|Mithaka Formation|46959|6|Mentioned|Table 1|||||||||
11984|Mithaka Formation|46973|6|Mentioned|p52|||||||||
11984|Mithaka Formation|47024|6|Mentioned|Table 1|||||||||
11984|Mithaka Formation|49027|4|Described|p19|||Mention p20.||||||06-NOV-06
11984|Mithaka Formation|60122|3|Fully described|p33|Middle Ordovician|Middle Ordovician|Of the Toko Gp. Conformable on Carlo Sandstone; conformable beneath Ethabuka Sandstone and Poodyea Formation. Max. thickness: 156m. Geological province: Georgina Basin. See also p4-5, p10 Tb. 1.||||||18-MAY-05
11984|Mithaka Formation|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Toko Group.  Gypsiferous shale and siltstone, calcareous siltstone, quartz sandstone, glauconitic and micaceous quartz sandstone, minor coquinite and granule conglomerate.||||||
11984|Mithaka Formation|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Gypsiferous shale and siltstone, calcareous siltstone, quartz sandstone, glauconitic and micaceous quartz sandstone, minor coquinite and granule conglomerate. Geological Province: southern Georgina Basin.||||||12-OCT-05
11984|Mithaka Formation|64068|3|Fully described|p77-78, p19|Late Ordovician|Late Ordovician|Diverse fauna. Deposited inshore of Carlo Sandstone barrier.||Of Toko Group.||Conformably and gradationally overlies Carlo Sandstone. Conformably and gradationally overlain by Ethabuka Sandstone, or unconformably by Cravens Peak beds.|Gypsiferous green shale, calcareous siltstone; minor calcareous sandstone, coquinite and granule conglomerate.|04-APR-12
11984|Mithaka Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
11984|Mithaka Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
11984|Mithaka Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
11984|Mithaka Formation|65489|5|Briefly described|p125|Ordovician|Ordovician|Georgina Basin.||||Overlies Carlo Sandstone. Is overlain by Ethabuka Formation.||
11984|Mithaka Formation|67323|5|Briefly described|GIS attrib tbl, p83, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also Solid Geology Map. West Toko Syncline, Georgina Basin.||Toko Group.||Overlies Carlo Sandstone. Is overlain by Ethubuka Sandstone.|Siltstone, arenite, quartzose, arenite, shale|
11984|Mithaka Formation|67402|6|Mentioned|p25, p25 tbl RRM3|Darriwillian|Darriwillian|Georgina Basin. Assessed to be a potential unconventional seal for Carbon dioxide storage. Deposited in a tidal or lagoonal environment associated with a barrier island system. Maximum thickness of 156m. See also p213 fig GRG3, p215-p217.||||Conformably overlies the Carlo Sandstone. Overlain by the Ethabuka Sandstone.|Siltstone and fine sandstone.|
11984|Mithaka Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Carlo Sandstone. Is overlain by Ethabuka Sandstone.||12-JUL-16
11984|Mithaka Formation|69443|4|Described|p28:7, 27, 29, 46|Late Ordovician|Late Ordovician|Casey in Smith (1963). Southern Georgina Basin. Poorly exposed. 20-156m thick. Mostly undescribed fossil fauna (listed). Late Gisbornian age. Low-energy marine lagoon deposits with limited tidal range. Potential seal for the Carlo Sandstone.||Toko Group.||Conformably and gradationally overlies Carlo Sandstone. Is overlain conformably and gradationally by Ethabuka Sandstone, or unconformably by Cravens Peak beds.|Thinly bedded gypsiferous shale, calcareous siltstone, minor calcareous, glauconitic and micaceous quartz sandstone, and minor coquinite and granule conglomerate.|12-JUL-16
11984|Mithaka Formation|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
11984|Mithaka Formation|69591|5|Briefly described|p87, p95-96|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. 60-120m thick. Contains a moderately diverse fauna (listed).||Toko Group.||Conformably and transitionally overlies Carlo Sandstone. Is overlain conformably by Ethabuka Sandstone.|Succession of brown and grey gypsiferous siltstone and sandstone, white glauconitic quartz sandstone, green gypsiferous shale, calcareous shale and thin coquinite. Sand increases up-section.|
11984|Mithaka Formation|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
11984|Mithaka Formation|69673|5|Briefly described|p118, p119 fig 94, p128, p136|Ordovician|Ordovician|120m thick.||Toko Group||Overlies Carlo Sandstone, overlain by Ethabuka Sandstone|Gypsiferous shale, calcareous siltstone and minor calcareous, glauconitic and micaceous quartz sandstone.|
11984|Mithaka Formation|70380|6|Mentioned|p745|Katian|Sandbian|Southern Georgina Basin.||||||
11984|Mithaka Formation|72297|5|Briefly described|p748|||Forms suitable cap rocks in the Toko Syncline, Georgina Basin.|||||Siltstone and mudstone.|
11984|Mithaka Formation|72503|6|Mentioned|p33|||Georgina Basin. Contains typical shallow-water [conodont] forms (e.g., Aurilobodus leptosomatus and Tangshanodus sp.).||||||
12080|Monastery Creek Phosphorite Member|22954|6|Mentioned|Fig3p9|Middle Cambrian|Ordian-Early Templetonia|||||||
12080|Monastery Creek Phosphorite Member|29940|6|Mentioned|p169|||||||||
12080|Monastery Creek Phosphorite Member|30242|6|Mentioned|p12|||See also Table 2 Clay mineralogy||||||
12080|Monastery Creek Phosphorite Member|32952|4|Described|p1190|||See also pp1192,1194,1196-1200 etc. M.Cambrian||||||07-NOV-06
12080|Monastery Creek Phosphorite Member|33111|6|Mentioned|p12|||||||||
12080|Monastery Creek Phosphorite Member|33482|6|Mentioned|p6|||Top of Beetle Creek Formation||||||
12080|Monastery Creek Phosphorite Member|35001|6|Mentioned|p263|||||||||
12080|Monastery Creek Phosphorite Member|36645|4|Described|p315|||Fig.3, p307.||||||07-NOV-06
12080|Monastery Creek Phosphorite Member|37572|4|Described|p158|||||||||
12080|Monastery Creek Phosphorite Member|38446|4|Described|p160|||||||||
12080|Monastery Creek Phosphorite Member|39690|6|Mentioned|p90|||||||||
12080|Monastery Creek Phosphorite Member|40852|5|Briefly described|p38|||||||||
12080|Monastery Creek Phosphorite Member|40856|5|Briefly described|p313|||||||||
12080|Monastery Creek Phosphorite Member|40857|5|Briefly described|p269|||See also Fig.21.6||||||
12080|Monastery Creek Phosphorite Member|41639|5|Briefly described|p3|||||||||
12080|Monastery Creek Phosphorite Member|42070|6|Mentioned|p4|||||||||
12080|Monastery Creek Phosphorite Member|42575|5|Briefly described|p334|||||||||
12080|Monastery Creek Phosphorite Member|44757|4|Described|p15||Middle Cambrian|(terminology not formalised with code) (lower Middle Cambrian) Described especially with respect to phosphorite.||||||
12080|Monastery Creek Phosphorite Member|45079|4|Described|p22|||See also p19. Member of Beetle Creek Formation.||||||02-APR-07
12080|Monastery Creek Phosphorite Member|50100|5|Briefly described|p22, p75|Cambrian|Cambrian|Referred to as the upper Monastery Creek Phosphorite Member of the Beetle Creek Formation.  Max. thickness: 38m.||||||02-APR-07
12080|Monastery Creek Phosphorite Member|60264|5|Briefly described|p575|Middle Cambrian|Middle Cambrian|Upper section of the Monastery Creek Formation.  Grainstone phosporite, chert, phosphatic and siliceous siltstone, shale, sandstone and phosphatic limestone; contains phosphatised fossils.  Max. thickness: 15m.||||||
12080|Monastery Creek Phosphorite Member|64068|4|Described|p62, p114|Middle Cambrian|Middle Cambrian|Potential oil source rock. Fossiliferous.||At top of Beetle Creek Formation.||Is conformably overlain by Inca Formation.|Siliceous and calcareous phosphorite, phosphatic chert, phosphatic and siliceous siltstone and shale, shale, foetid phosphatic limestone.|05-APR-12
12080|Monastery Creek Phosphorite Member|69573|6|Mentioned|p656|||Features Cambrian Stage 5 fossil sites.||Beetle Creek Formation.||||
12080|Monastery Creek Phosphorite Member|70723|6|Mentioned|p30|Cambrian|Cambrian|Georgina Basin.|510 Ma|||||
12080|Monastery Creek Phosphorite Member|72321|6|Mentioned|Fig 2|Drumian|Wulian|Burke River Structural Belt, Georgina Basin. Australian stages: Templetonian to Floran.||||Overlies Beetle Creek Formation. Overlain by Inca Formation.||
12080|Monastery Creek Phosphorite Member|73418|4|Described|p3-5|Miaolingian|Miaolingian|Georgina Basin. Abbreviated to MCPM in text. Also referred to as Simpson Creek Member. Deposition in shallow marine facies with wave and current action. Pelletal phosphorites in southern parts (Burke River Structural Belt) lack terrigenous material and can contain over 0.5 wt% REE. MCPM in southern parts is typically 8-14 m thick, maximum thickness of 38 m. Greater proportions of non-pelletal apatite mudstone and terrigenous material occur in central to northern parts (Undilla sub-basin), depositional environmental was littoral, emergent to shallow marine facies. Average thickness of 6 m and maximum thickness of 13 m in northern parts. Deformed in southern part of basin.||Beetle Creek Formation||Overlies Lower Siltstone Member|Contains largely continuous sedimentary beds of pelletal phosphorites, interbedded with phosphatic cherts and siltstones, and very thin bands of apatitic mudstone (collophane mudstone) near the top of the phosphorite unit.|
12115|Monsildale Granodiorite|22845|6|Mentioned|p69|Triassic|Permian|||||||
12115|Monsildale Granodiorite|22846|3|Fully described|p6,26-35|Middle Triassic|Late Permian|Contains 2 phases, with a more felsic older phase to the north and a southern more mafic younger phase.||||||
12115|Monsildale Granodiorite|23609|4|Described|p13-15|||Also see p17. Geochemical Classification. North D'Aguilar Block.||||||
12115|Monsildale Granodiorite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
12115|Monsildale Granodiorite|35101|3|Fully described|p69|||||||||
12115|Monsildale Granodiorite|37252|6|Mentioned|Map legend|Permian|Permian|||||||
12115|Monsildale Granodiorite|39445|5|Briefly described|Table 12|||||||||
12115|Monsildale Granodiorite|41917|6|Mentioned|p522|||||||||
12115|Monsildale Granodiorite|43588|6|Mentioned|p31|Early Triassic|Late Permian|||||||
12115|Monsildale Granodiorite|60077|5|Briefly described|Map legend|Triassic|Permian|Grey granodiorite, gabbro, diorite, quartz diorite.||||||
12115|Monsildale Granodiorite|60370|5|Briefly described|Map Legend|Triassic|Permian|Biotite-hornblende granodiorite; biotite-hornblende quartz diorite; hornblende diorite; olivine gabbro.||||||27-OCT-08
12115|Monsildale Granodiorite|61782|6|Mentioned|p278|||Age: ~253Ma (Sliwa 1994).||||||
12115|Monsildale Granodiorite|68679|5|Briefly described|p409, p411|Late Triassic|Late Triassic|Kwiecien (1996). A small intrusion (~36 km2), but heterogeneous in texture, mineralogy, geochemistry and age; has a complex petrogenesis assigned to two distinct phases. Several age determinations given.|253.1 +/- 10 Ma to 227 +/- 3 Ma.||||Northern (crustal contraction) phase: granites, granodiorites, diorites and gabbros are subduction-related and may be genetically related. The southern (?attenuation) phase has granodiorite, diorite and gabbro, each with a different origin.|
12129|Monteagle Quartzite|22557|6|Mentioned|p567,569|||||||||
12129|Monteagle Quartzite|23078|5|Briefly described|p708|||||||||
12129|Monteagle Quartzite|23854|5|Briefly described|p859 Fig 3|Neoproterozoic|Neoproterozoic|||||||
12129|Monteagle Quartzite|42747|5|Briefly described|p33, Fig.3|||of Anakie Metamorphic Group||||||
12129|Monteagle Quartzite|43029|6|Mentioned|p19|||||||||
12129|Monteagle Quartzite|43204|5|Briefly described|Map Legend||Neoproterozoic|Neoproterozoic or Early Cambrian. Anakie Inlier||||||23-DEC-11
12129|Monteagle Quartzite|43213|3|Fully described|p8,p20-22, p37-39, p130-140, p183,p236, |||See also p240, p245. Named after Monteagle Holding. Outcrop area, type area and geophysical properties described. Deformation structures detailed. Hosts the very large but low-grade Moorlands gold prospect.||Unit in Anakie Metamorphic Group.||Structurally overlies Rolfe Creek Schist. Is overlain by Wynyard Metamorphics. Is overlain unconformably by Silver Hills Volcanics.|White, strongly foliated, fine- to very coarse-grained, medium- to very thick-bedded quartzite, interlayered with mica schist and phyllite with local well-preserved sedimentary layering.|
12129|Monteagle Quartzite|43861|2|Defined|25; Fig1p26; p28-30|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group.||||||23-JUN-15
12129|Monteagle Quartzite|66085|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Unit in Anakie Metamorphic Group. White, fine- to coarse-grained, strongly foliated quartzite and fine-grained mica schist grading to phyllite.||||||
12129|Monteagle Quartzite|66851|5|Briefly described|p915, 917, 918, 922|||Bedding is defined by alternating psammitic and schist layers. Only one foliation is present in most exposures, from three deformation events. D2 produced mylonitic foliation and grainsize reduction in quartz. Tight, rootless, F2 folds are common.||Unit in Anakie Metamorphic Group.||||18-JAN-17
12129|Monteagle Quartzite|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.||Conformably overlies Rolfe Creek Schist. Is conformably overlain by Wynyard Metamorphics.|White, fine- to coarse-grained, strongly foliated quartzite and fine-grained mica schist grading to phyllite.|23-JUN-15
12129|Monteagle Quartzite|68482|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Anakie Province.||Of the Anakie Metamorphic Group.||Conformably overlain by the Wynyard Metamorphics. Conformably underlain by the Rolfe Creek Schist.|White, fine to coarse-grained, strongly foliated quartzite and fine-grained mica schist grading to phyllite.|
12129|Monteagle Quartzite|68731|5|Briefly described|p120 Fig 3.6, p121 Fig 3.7, p122, p126|Early Cambrian|Neoproterozoic|~ 3 km thick. Detailed lithology discussed. See also Monteagle quartzite. Age constrained by the Anakie Metamorphic Group.||Of the Anakie Metamorphic Group.||Underlain by the Rolfe Creek Schist. Overlain by the Wynyard Metamorphics.|Comprises abundant quartzite interlayered with psammitic and mica schist.|
12129|Monteagle Quartzite|68900|5|Briefly described|p6, p10|||Drummond Basin.||||Overlies the Rolfe Creek Schist. Overlain by the Wynyard Metamorphics.|White, strongly foliated quartzite interlayered with mica schist and phyllite.|
12129|Monteagle Quartzite|70749|5|Briefly described|p43|Cambrian|Neoproterozoic|Anakie Province.||Anakie Metamorphic Group.||||
12129|Monteagle Quartzite|71966|6|Mentioned|p990|Cambrian|Neoproterozoic|Geological province: Anakie Province, Thomson Orogen.||||||
12136|Montgomery Range Igneous Complex|23032|4|Described|p41,42||Carboniferous|||||||
12136|Montgomery Range Igneous Complex|23424|5|Briefly described|Table 8.1 p339.|Permian|Carboniferous|Intrudes Bundock Creek Group. Age: Carboniferous or ?Permian.||||||
12136|Montgomery Range Igneous Complex|23430|5|Briefly described|p479|||||||||
12136|Montgomery Range Igneous Complex|23431|6|Mentioned|p541|||Kennedy Province||||||
12136|Montgomery Range Igneous Complex|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 74. I-Type.||||||
12136|Montgomery Range Igneous Complex|24577|6|Mentioned|p762|||||||||
12136|Montgomery Range Igneous Complex|41260|3|Fully described|p95|||||||||
12136|Montgomery Range Igneous Complex|41679|6|Mentioned|p251|||||||||
12136|Montgomery Range Igneous Complex|41719|6|Mentioned|Fig.1|||||||||
12136|Montgomery Range Igneous Complex|41739|1|Redefined|p305|Permian|Late Carboniferous|||||||
12136|Montgomery Range Igneous Complex|42054|6|Mentioned|p273|||||||||
12136|Montgomery Range Igneous Complex|42693|5|Briefly described|map legend|Carboniferous||||||||
12136|Montgomery Range Igneous Complex|42709|6|Mentioned|map legend|||||||||
12136|Montgomery Range Igneous Complex|42752|5|Briefly described|p48, Fig.3 p47|||||||||
12136|Montgomery Range Igneous Complex|42933|3|Fully described|p174|||||||||
12136|Montgomery Range Igneous Complex|43259|4|Described|Appendix 1,p20.||Carboniferous|originally Montgomery Range Rhyolite Porphyry. Possibly related to Pamplemousse Complex.||||||
12136|Montgomery Range Igneous Complex|43286|5|Briefly described|Map Legend||Carboniferous|||||||
12136|Montgomery Range Igneous Complex|50200|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
12136|Montgomery Range Igneous Complex|63154|5|Briefly described|p281 Fig. 3||Late Carboniferous|Geological province: Broken River Province/Graveyard Creek Subprovince.||||||11-APR-07
12136|Montgomery Range Igneous Complex|68336|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince. The four (un-named) units are mapped separately.|||||Pink, sparsely to abundantly porphyritic microgranite and rhyolite; pink, fine- to medium-grained, biotite-hornblende granodiorite and biotite to hornblende-biotite granite, locally granophyric.|
12136|Montgomery Range Igneous Complex|68341|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Graveyard Creek Subprovince. The four (un-named) units are mapped separately.|||||Pink, sparsely to abundantly porphyritic microgranite and rhyolite; pink, fine- to medium-grained, biotite-hornblende granodiorite and biotite to hornblende-biotite granite, locally granophyric.|
12136|Montgomery Range Igneous Complex|68410|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Contains 3 unnamed subunits.|||||Pink sparsely to abundantly porphyritic microgranite; pink to grey, fine to medium-grained biotite-hornblende granodiorite; pink, fine to medium-grained, biotite to hornblende-biotite granite, locally granophyric.|
12136|Montgomery Range Igneous Complex|68478|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Kennedy Province. The 2 facies are mapped separately.|||||Pink to grey, fine to medium-grained biotite-hornblende granodiorite; pink, sparsely to abundantly porphyritic microgranite.|
12136|Montgomery Range Igneous Complex|68479|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Kennedy Province. The 2 facies are mapped separately.|||||Pink to grey, fine to medium-grained biotite-hornblende granodiorite; pink, sparsely to abundantly porphyritic microgranite.|
12136|Montgomery Range Igneous Complex|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit (in part), as well as the Almaden, Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Ootann (in part) and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk.||||||
12136|Montgomery Range Igneous Complex|69030|6|Mentioned|p6|Carboniferous|Carboniferous|Bundock Basin (Broken River Province).||||||
12136|Montgomery Range Igneous Complex|69079|6|Mentioned|p63|||Proposed as a distant igneous source for auriferous fluids involved in the Amanda Bel Goldfield; alternatively as the heat source for gold-scavenging metamorphic fluids.||||||
12136|Montgomery Range Igneous Complex|69592|6|Mentioned|p277|Permian|Pennsylvanian|Stocks, sills and lopoliths. Relationship to deformations in Graveyard Creek Subprovince and Bundock Basin discussed.||||||
12136|Montgomery Range Igneous Complex|69593|5|Briefly described|p494, p496, p512|||Broken River Province. Forms numerous intrusives in the Bindock Basin. Unassigned. Age uncertain; probably Early or Mid-Carboniferous to Permian (?). Sm-Nd isotope data tabulated.|315 Ma.||||Dominated by biotite granite and granophyre, subordinate microgranite, granodiorite, rhyolite and dacite, locally hornblende-bearing. I-type.|
12147|Montserrat Granophyre|40896|5|Briefly described|p53|||||||||
12147|Montserrat Granophyre|44778|4|Described|p128,132,134,135|||(Post Triassic - pre Eocene-Oligocene)||||||
12147|Montserrat Granophyre|44781|14|Not recorded|p362|||||||||
12170|Mooga Sandstone|730|6|Mentioned|p24.|||Fluviatile.||||||11-NOV-14
12170|Mooga Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497|Early Cretaceous|Early Cretaceous|N Surat Basin. 50-100m thick. Basal section is permeable and acts as a major aquifer.||||Grades laterally into upper part of Hooray Sandstone.|Quartzose, sub-labile, upward-fining fluvial sandstone, with interbeds of siltstone and mudstone at the top.|
12170|Mooga Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
12170|Mooga Sandstone|22757|5|Briefly described|Table6,p11||Early Cretaceous|60 m. Surat Basin.||||||
12170|Mooga Sandstone|22857|4|Described|p295, p296-7 Tb.22.1, p546 Tb.A1.12|Hauterivian|Berriasian|Of the Blythesdale Group. Fine-grained sublabile to quartzose arenite with interbedded siltstone and shale. Equivalent of Hooray Sandstone (Eromanga Basin). Max. thickness: 56m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
12170|Mooga Sandstone|22865|4|Described|p295,Table22.1p296-7|Valanginian|Berriasian|||||||
12170|Mooga Sandstone|23053|6|Mentioned|Fig10p17,26|Valanginian|Tithonian|||||||
12170|Mooga Sandstone|23056|6|Mentioned|9|||Geol province Eromanga Basin||||||
12170|Mooga Sandstone|23818|6|Mentioned|140|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
12170|Mooga Sandstone|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 140m.||||||
12170|Mooga Sandstone|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
12170|Mooga Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|29379|6|Mentioned|Fig.11|||Showing oil company usage compared with Freytag(1966)&Forbes(1966).||||||
12170|Mooga Sandstone|29387|6|Mentioned|Table 5|||||||||
12170|Mooga Sandstone|29393|6|Mentioned|Table 4|||||||||
12170|Mooga Sandstone|29591|6|Mentioned|p77|||||||||
12170|Mooga Sandstone|29721|6|Mentioned|Table 246|||||||||
12170|Mooga Sandstone|30021|6|Mentioned|p87|||||||||
12170|Mooga Sandstone|30022|6|Mentioned|p28|||||||||
12170|Mooga Sandstone|30024|6|Mentioned|p332|||||||||
12170|Mooga Sandstone|30540|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
12170|Mooga Sandstone|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30695|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30696|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30697|6|Mentioned|p34|||Major aquifer present||||||
12170|Mooga Sandstone|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30699|6|Mentioned|p53|||Middle Jurassic - Early Cretaceous. Stratigraphy||||||
12170|Mooga Sandstone|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30702|4|Described|p48|||See also p49-51, Table 1, Fig.1,2.||||||13-JUN-22
12170|Mooga Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
12170|Mooga Sandstone|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|31098|5|Briefly described|Table 1|||Lower Cretaceous||||||
12170|Mooga Sandstone|31116|4|Described|p40|||Cretaceous. See also Table 2||||||
12170|Mooga Sandstone|31369|6|Mentioned|Table 4|||Cretaceous||||||
12170|Mooga Sandstone|31376|6|Mentioned|p4|||||||||
12170|Mooga Sandstone|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32797|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33070|4|Described|Table 2|||L.Cret.||||||
12170|Mooga Sandstone|33071|6|Mentioned|p6|||L.Cret.||||||
12170|Mooga Sandstone|33075|6|Mentioned|p451|||||||||
12170|Mooga Sandstone|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33090|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33091|5|Briefly described|p7|||Stratigraphy||||||
12170|Mooga Sandstone|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
12170|Mooga Sandstone|33367|6|Mentioned|p17|||||||||
12170|Mooga Sandstone|33414|6|Mentioned|p214|||||||||
12170|Mooga Sandstone|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33523|6|Mentioned|p27|||||||||
12170|Mooga Sandstone|33672|6|Mentioned|p44|||||||||
12170|Mooga Sandstone|33828|6|Mentioned|Table 3|||||||||
12170|Mooga Sandstone|33939|6|Mentioned|p412|||Blythesdale Group.||||||
12170|Mooga Sandstone|33971|6|Mentioned|Fig.29|||Strat. table.||||||
12170|Mooga Sandstone|34254|6|Mentioned|p491|||||||||
12170|Mooga Sandstone|34543|6|Mentioned|p98|||||||||
12170|Mooga Sandstone|34611|6|Mentioned|p140|||Jurassic. Correlation chart. Fig.65.||||||
12170|Mooga Sandstone|34613|4|Described|Table 4|||||||||
12170|Mooga Sandstone|35793|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|35937|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|36243|6|Mentioned|Table 7A|||||||||
12170|Mooga Sandstone|36570|4|Described|p49|||See also p45, Fig.9, p60.||||||13-JUN-22
12170|Mooga Sandstone|36751|6|Mentioned|p488|||||||||
12170|Mooga Sandstone|36827|6|Mentioned|p83|||||||||
12170|Mooga Sandstone|37117|5|Briefly described|p313|||||||||
12170|Mooga Sandstone|37995|4|Described|p65|||||||||
12170|Mooga Sandstone|38068|6|Mentioned|p71|||||||||
12170|Mooga Sandstone|39211|5|Briefly described|p31|||See also Fig.3||||||
12170|Mooga Sandstone|39212|5|Briefly described|p17|||Early Neocomian. See also p15.||||||13-JUN-22
12170|Mooga Sandstone|39215|6|Mentioned|p51|||Spore/pollen record||||||
12170|Mooga Sandstone|39218|6|Mentioned|p48|||Flora||||||
12170|Mooga Sandstone|39315|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39445|5|Briefly described|Table 10|||||||||
12170|Mooga Sandstone|39494|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39914|6|Mentioned|p2|||||||||
12170|Mooga Sandstone|39943|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|39998|6|Mentioned|p192|||||||||
12170|Mooga Sandstone|40030|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|40245|6|Mentioned|Table 2|||||||||
12170|Mooga Sandstone|40249|6|Mentioned|p38|||Mention P41||||||
12170|Mooga Sandstone|40250|6|Mentioned|Fig.1|||||||||
12170|Mooga Sandstone|40541|3|Fully described|p110|||||||||
12170|Mooga Sandstone|40544|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|40666|4|Described|p358|||||||||
12170|Mooga Sandstone|40675|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|40687|6|Mentioned|p417|||||||||
12170|Mooga Sandstone|40926|6|Mentioned|p13|||||||||
12170|Mooga Sandstone|41057|6|Mentioned|p61|||||||||
12170|Mooga Sandstone|41060|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41061|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|41064|6|Mentioned|p60|||||||||
12170|Mooga Sandstone|41187|6|Mentioned|Fig.2|||||||||
12170|Mooga Sandstone|41188|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41210|5|Briefly described|Fig.3|||||||||
12170|Mooga Sandstone|41216|6|Mentioned|Fig.18|||||||||
12170|Mooga Sandstone|41246|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|41247|6|Mentioned|Fig.7|||||||||
12170|Mooga Sandstone|41266|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41681|6|Mentioned|p16|||||||||
12170|Mooga Sandstone|41712|6|Mentioned|p282|||||||||
12170|Mooga Sandstone|41992|4|Described|Fig.2 P183|||||||||
12170|Mooga Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
12170|Mooga Sandstone|42135|6|Mentioned|Fig.6 P357|||||||||
12170|Mooga Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
12170|Mooga Sandstone|42494|5|Briefly described|Table 1 P24|||||||||
12170|Mooga Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
12170|Mooga Sandstone|43000|5|Briefly described|Fig.5,p112|||Of Blythesdale Group.||||||16-SEP-08
12170|Mooga Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
12170|Mooga Sandstone|43404|14|Not recorded|Table p11|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group.  Misspelling of Mooga Formation?||||||
12170|Mooga Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
12170|Mooga Sandstone|43991|5|Briefly described|p50|Cretaceous|Jurassic|Part of the "Blythesdale Group".||||||
12170|Mooga Sandstone|43995|14|Not recorded|p13,57,58,Fig.5|||Part of Blythesdale Group.||||||
12170|Mooga Sandstone|44021|14|Not recorded|p233,238|||Equivalent to "Hooray Sandstone" in Eromanga Basin.||||||
12170|Mooga Sandstone|44087|14|Not recorded|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44088|4|Described|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44091|14|Not recorded|p60||Cretaceous|||||||
12170|Mooga Sandstone|44171|14|Not recorded|p194|||||||||
12170|Mooga Sandstone|44375|14|Not recorded|p310,311|||Aquifer.||||||
12170|Mooga Sandstone|44377|1|Redefined|p2,7-11,15|||Redefined as Mooga Sandstone Member. Of Blythesdale Formation.||||||
12170|Mooga Sandstone|44915|14|Not recorded|p18|||Ref. to Day 1964, Whitehouse 1955, Vine and Day 1965. Equivalent to Village Well Formation in South Australia. No age given.||||||
12170|Mooga Sandstone|45103|6|Mentioned|p6|||||||||
12170|Mooga Sandstone|45110|2|Defined|p105|Early Cretaceous|Early Cretaceous|See also p9 and p24.||||||13-JUN-22
12170|Mooga Sandstone|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
12170|Mooga Sandstone|46791|5|Briefly described|p42|||||||||
12170|Mooga Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
12170|Mooga Sandstone|46984|6|Mentioned|Table 1|||||||||
12170|Mooga Sandstone|48634|14|Not recorded|p6,20||Late Jurassic|See also Fig.2,6, Pl.1,2 p5,19. Upper Jurassic. (G54-14).||||||
12170|Mooga Sandstone|48919|4|Described|p70|||See also Table 5||||||
12170|Mooga Sandstone|48920|6|Mentioned|Table 7|||Refers Exon & Vine (1970)||||||
12170|Mooga Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
12170|Mooga Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
12170|Mooga Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
12170|Mooga Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|63979|5|Briefly described|p40, p44|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
12170|Mooga Sandstone|64197|6|Mentioned|p630 Fig.7|Early Cretaceous|Early Cretaceous|||||Underlies Bungil Formation; overlies Orallo Formation.||
12170|Mooga Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|64856|3|Fully described|p79, p95-98|Valanginian|Berriasian|Surat Basin. Of Reeves (1947). Renamed Mooga Sandstone Member (of Blythesdale Formation) by Day (1964), with a type area along Blyth Creek, 24-34km ENE of Roma. Renamed back to Mooga Sandstone by Exon and Vine (1970) with a new type area near the junction of Bungil and Mooga-Mooga Creeks, 16km N of Roma. Overlies Orallo Formation conformably, locally disconformably. Grades into upper Hooray Sandstone to the west. Is overlain conformably by Bungil Formation. Age from palynofloral units APK1, 21. <168m. Sublabile to quartzose sandstone, minor siltstone.|| ||||29-NOV-17
12170|Mooga Sandstone|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|64858|6|Mentioned|p187-188|||See also Mooga Formation.||||||16-MAR-12
12170|Mooga Sandstone|65003|4|Described|p1,p13, p14, p25|Cretaceous|Cretaceous|||||Overlies the Orallo Formation and the Boondooma Igneous Complex|Fine to medium-grained fawn sandstone that weathers yellow and brown.|
12170|Mooga Sandstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin. Underlies the Bungil Formation, overlies the Orallo Formation.||||||22-MAR-12
12170|Mooga Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Orallo Formation, underlies the Bungil Formation.||||||
12170|Mooga Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
12170|Mooga Sandstone|65116|5|Briefly described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Bungil Formation, Overlies the Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|65119|5|Briefly described|Fig 2 p503, Fig 7- 8, 14, 16-19|Early Cretaceous |Early Cretaceous|Surat Basin. Quartzose to lithic sandstone, some mud and siltstone, up to 300m thick.||||||
12170|Mooga Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|66915|5|Briefly described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Surat Basin.||||||12-JAN-17
12170|Mooga Sandstone|67133|5|Briefly described|p17, p21|Cretaceous|Cretaceous|Not included in this study. Part of the final cycle of deposition under fluvial conditions in the Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|67402|4|Described|p146 fig SRT3, p148, p156|Barremian|Tithonian|Surat Basin. Deposited in a braided or meandering fluvial environment. Approximately 178m thick.||Blythesdale Group||Overlies the Orallo Formation. Overlain by the Bungil Formation.|Sandstone, minor clay, siltstone and mudstone.|
12170|Mooga Sandstone|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Bungil Formation. Underlain by Orallo Formation.||
12170|Mooga Sandstone|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68004|6|Mentioned|p174, p175.|||Major aquifer for water production; excellent quality reservoir. Sealed by Wallumbilla Formation shales. A major hydrocarbon exploration target. See also reference to Mooga Formation p87.||||||
12170|Mooga Sandstone|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluvial environment.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone; minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Early Cretaceous|Surat Basin (NSW and QLD): contains plant macrofossils in the latter.||||Overlies Orallo Formation|Silty sandstone.|14-SEP-17
12170|Mooga Sandstone|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Longsight Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
12170|Mooga Sandstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Early Cretaceous|Fluvial deposits. One of the main artesian aquifers in the map area.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone, minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68734|6|Mentioned|p218 Fig.2, p221 Fig.3|||Surat Basin. Fluvial. Pre-Barremian age.||||||16-JAN-17
12170|Mooga Sandstone|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Orallo Formation. Overlain by the Bungil Formation.||
12170|Mooga Sandstone|69594|5|Briefly described|p519, p527, p537-538, p573|Hauterivian|Valanginian|Reeves (1947); Exon and Vine (1970). Northern Surat Basin. Braided to meandering stream deposits. Up to 168m thick. An important local aquifer in the Roma district.||||Conformably overlies Orallo Formation, locally disconformably. Is overlain conformably by Bungil Formation. Equivalent to/laterally grades into Hooray Sandstone and Kumbarilla beds.|Three subunits: a lower sublabile to quartzose sandstone that is commonly conglomeratic; a middle mudstone; and an upper subunit of interbedded fine sublabile sandstone and siltstone.|
12170|Mooga Sandstone|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
12170|Mooga Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
12170|Mooga Sandstone|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal.||||||
12170|Mooga Sandstone|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p33, p80|Early Cretaceous|Jurassic|Surat Basin.  Aquifer: generally artesian. Appears as Mooga Sandstone Member in Fig.2.6.||||Overlies Walloon Coal Measures and Orallo Formation. Is overlain by Bungil Formation or Cadna-owie Formation.||
12170|Mooga Sandstone|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Berriasian-Valanginian.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Orallo FZ. Is overlain by Kingull Member (Bungil FZ).||
12170|Mooga Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Cretaceous|Shown as located in the Surat Basin, both Qld and NSW.||||Overlies Orallo Formation||
12170|Mooga Sandstone|73113|5|Briefly described|p. 22-24, 36-37, 41, 43, 69, 80, 88...|||Surat Basin. Regional aquifer. More locations: p. 116-117, 119, 146, 151-152, 160, 169-173, 177-178, 191.||||||
12170|Mooga Sandstone|73193|6|Mentioned|p369|Hauterivian|Valanginian|Surat Basin.||||Underlain by Orallo Formation. Overlain by Bungil Formation.||
12187|Moolayember Formation|13516|5|Briefly described|p159 fig 8, p160-164, p169, p170, p138|Middle Triassic|Middle Triassic|From Bowen Basin, Galilee Basin. Age: APT3|||Includes Snake Creek Mudstone Member, ?Showgrounds Sandstone Member|Diachronous contact with underlying Showgrounds Sandstone.||
12187|Moolayember Formation|22464|6|Mentioned|p9||Middle Triassic|Overlies Clematis Sandstone||||||
12187|Moolayember Formation|22757|4|Described|Table4,p9|Late Triassic|Middle Triassic|130 m thick. Conformable on Clematis Sandstone.||||||27-OCT-08
12187|Moolayember Formation|22857|6|Mentioned|p315 Fig. 22.8|||||||||
12187|Moolayember Formation|22865|6|Mentioned|Fig22.8p315|||||||||
12187|Moolayember Formation|22973|5|Briefly described|p13 Fig.2 (i)|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
12187|Moolayember Formation|22976|5|Briefly described|p42 Fig.4|Triassic|Triassic|||||||
12187|Moolayember Formation|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
12187|Moolayember Formation|23052|5|Briefly described|Map Legend|Triassic|Triassic|||||||
12187|Moolayember Formation|23161|4|Described|p33 table4 fig11||Triassic|||||||
12187|Moolayember Formation|23425|6|Mentioned|p391.|||||||||
12187|Moolayember Formation|23430|5|Briefly described|p514|||Underlying Unit Clematis Group. Bowen Basin Province.||||||
12187|Moolayember Formation|23740|6|Mentioned|p1221|||Geological Province: Bowen Basin||||||
12187|Moolayember Formation|23883|5|Briefly described|p129 Fig. 11.2|Triassic|Triassic|Age: 251-205Ma.  Geological Province: Great Australian Superbasin.||||||
12187|Moolayember Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Triassic|Geological Province: Great Artesian Basin.||||||
12187|Moolayember Formation|24069|5|Briefly described|p284|Middle Triassic|Middle Triassic|Geological Province: Surat Basin.||||||
12187|Moolayember Formation|24071|5|Briefly described|p319|Triassic|Triassic|Geological Province: Galilee Basin.||||||
12187|Moolayember Formation|24077|5|Briefly described|p411 Tb. 2|Middle Triassic|Early Triassic|Of Mimosa Group.  Max. thickness: 315m.  Geological Province: Bowen Basin.||||||
12187|Moolayember Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
12187|Moolayember Formation|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Age: <235Ma. Overlies the Clematis Group. Geological Province: Bowen Basin.||||||29-JAN-08
12187|Moolayember Formation|24159|5|Briefly described|p148, Fig.2, p149|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin. Overlying Unit: Unconformity with Precipice Sandstone.||||||
12187|Moolayember Formation|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|28288|14|Not recorded|?|||||||||
12187|Moolayember Formation|29385|6|Mentioned|p80|||See also P81,82||||||
12187|Moolayember Formation|29387|6|Mentioned|Table 3|||Also Table 4. Triassic.||||||
12187|Moolayember Formation|29388|6|Mentioned|p62|||Stratigraphy.||||||
12187|Moolayember Formation|29389|6|Mentioned|p17|||||||||
12187|Moolayember Formation|29391|6|Mentioned|Table 4|||See P19.||||||
12187|Moolayember Formation|29393|6|Mentioned|Table 2|||Triassic.||||||
12187|Moolayember Formation|29410|6|Mentioned|p274|||Geological map. Triassic.||||||
12187|Moolayember Formation|29411|6|Mentioned|p202|||||||||
12187|Moolayember Formation|29591|6|Mentioned|Table 15|||||||||
12187|Moolayember Formation|29721|6|Mentioned|p65|||||||||
12187|Moolayember Formation|29869|6|Mentioned|p37|||||||||
12187|Moolayember Formation|30102|4|Described|p14|||See also P10,12,15. May occur as a shale interval under the Hutton Sandstone in P.S. Glenaras 1.||||conformably overlies Clematis Sandstone. Unconformably overlain by Hutton Sandstone||08-FEB-13
12187|Moolayember Formation|30103|6|Mentioned|p8|||||||||
12187|Moolayember Formation|30455|5|Briefly described|p1|||See also P2-3. Triassic age||||||
12187|Moolayember Formation|30456|6|Mentioned|p95|||||||||
12187|Moolayember Formation|30457|6|Mentioned|p96|||||||||
12187|Moolayember Formation|30458|6|Mentioned|p3|||Middle Triassic age||||||
12187|Moolayember Formation|30459|6|Mentioned|p309|||||||||
12187|Moolayember Formation|30460|6|Mentioned|p1|||See also P3-7,9-16,19,20,22,26, Fig.1. Triassic age||||||
12187|Moolayember Formation|30465|6|Mentioned|p4|||||||||
12187|Moolayember Formation|30466|6|Mentioned|p4|||Triassic age||||||
12187|Moolayember Formation|30468|6|Mentioned|p383|||||||||
12187|Moolayember Formation|30472|6|Mentioned|p134|||Correlation||||||
12187|Moolayember Formation|30473|6|Mentioned|p377|||Similar miospore assemblage to that in Esk Formation.||||||
12187|Moolayember Formation|30475|6|Mentioned|p164|||||||||
12187|Moolayember Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
12187|Moolayember Formation|30546|14|Not recorded|p107|Late Triassic|Middle Triassic|Correlation.||||||
12187|Moolayember Formation|30565|6|Mentioned|p134|||||||||
12187|Moolayember Formation|30691|4|Described|p14|||See also Table 4,6. Middle-Upper Triassic age||||||
12187|Moolayember Formation|30692|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|30696|4|Described|Table 3|||Middle-Upper Triassic||||||
12187|Moolayember Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
12187|Moolayember Formation|30701|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
12187|Moolayember Formation|30853|6|Mentioned|p9|||Penetrated in Bury No.1||||||
12187|Moolayember Formation|30854|4|Described|Table 3|||Middle-Upper Triassic age||||||
12187|Moolayember Formation|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
12187|Moolayember Formation|31079|6|Mentioned|Fig. 6|||||||||
12187|Moolayember Formation|31115|4|Described|p32|||See also P33-34. Triassic||||||
12187|Moolayember Formation|31116|4|Described|p20|||See also P1. Middle Triassic||||||
12187|Moolayember Formation|31117|6|Mentioned|p378|||Mid Triassic||||||
12187|Moolayember Formation|31120|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|31121|6|Mentioned|p388|||||||||
12187|Moolayember Formation|31145|6|Mentioned|p7|||||||||
12187|Moolayember Formation|31305|6|Mentioned|Fig. 1|||||||||
12187|Moolayember Formation|31369|4|Described|p31|||See also P32-40. Triassic.||||||
12187|Moolayember Formation|31425|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|31553|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|31979|6|Mentioned|p22|||||||||
12187|Moolayember Formation|32136|6|Mentioned|p2|||Geol. map near Mundubbera No.1. Triassic||||||
12187|Moolayember Formation|32138|6|Mentioned|p393|||||||||
12187|Moolayember Formation|32193|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|32276|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper Triassic.M - U||||||
12187|Moolayember Formation|32490|4|Described|Table 1|||U.-M.Triassic||||||
12187|Moolayember Formation|32493|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|32553|4|Described|p40|||||||||
12187|Moolayember Formation|32577|6|Mentioned|p25|||Mid. or Late Triassic||||||
12187|Moolayember Formation|32944|6|Mentioned|p703|||Triassic||||||
12187|Moolayember Formation|33059|4|Described|Table 1|||See also Fig.4. Middle Triassic||||||
12187|Moolayember Formation|33078|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33079|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33086|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33091|5|Briefly described|p8|||Stratigraphy||||||
12187|Moolayember Formation|33092|5|Briefly described|p6|||Strat. table||||||
12187|Moolayember Formation|33096|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33366|6|Mentioned|Fig.3|||Triassic.||||||
12187|Moolayember Formation|33372|4|Described|p21|||From wells. Mention P16.||||||
12187|Moolayember Formation|33381|6|Mentioned|p115|||Triassic.||||||
12187|Moolayember Formation|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||08-FEB-13
12187|Moolayember Formation|33530|5|Briefly described|Table 1|||Middle Triassic||||||
12187|Moolayember Formation|33638|6|Mentioned|p8|||||||||
12187|Moolayember Formation|33639|5|Briefly described|p10|||M.-U.Triass.||||||
12187|Moolayember Formation|33640|4|Described|Table 3|||Triassic.||||||
12187|Moolayember Formation|33644|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33645|6|Mentioned|Map legend|Triassic|Triassic|Mimosa Gp.||||||
12187|Moolayember Formation|33646|5|Briefly described|p11|||||||||
12187|Moolayember Formation|33647|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33648|5|Briefly described|p18|||||||||
12187|Moolayember Formation|33672|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|33673|4|Described|p287|||||||||
12187|Moolayember Formation|33675|4|Described|p412|||Lithology.||||||
12187|Moolayember Formation|33774|6|Mentioned|p42|||Correlation||||||
12187|Moolayember Formation|34009|6|Mentioned|p109|||||||||
12187|Moolayember Formation|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
12187|Moolayember Formation|34061|6|Mentioned|p53|||||||||
12187|Moolayember Formation|34065|6|Mentioned|p9|||Triassic||||||
12187|Moolayember Formation|34091|6|Mentioned|p4|||Triassic||||||
12187|Moolayember Formation|34133|6|Mentioned|p1|||Triassic. See also PP2-5,28||||||
12187|Moolayember Formation|34172|6|Mentioned|p53|||Triassic.||||||
12187|Moolayember Formation|34174|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|34212|6|Mentioned|p1|||See also PP2,3,4 etc. Upper Triassic.||||||
12187|Moolayember Formation|34218|6|Mentioned|p9|||Triassic||||||
12187|Moolayember Formation|34254|6|Mentioned|p484|||||||||
12187|Moolayember Formation|34314|5|Briefly described|Table 3|||Triassic||||||
12187|Moolayember Formation|34391|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper TriassicM - U||||||
12187|Moolayember Formation|34408|6|Mentioned|p185|||On table||||||
12187|Moolayember Formation|34452|6|Mentioned|p1|||M.Triassic. See also P5||||||
12187|Moolayember Formation|34543|6|Mentioned|p98|||||||||
12187|Moolayember Formation|34613|4|Described|Table 3|||||||||
12187|Moolayember Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
12187|Moolayember Formation|35095|6|Mentioned|p115|||||||||
12187|Moolayember Formation|35141|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|35148|6|Mentioned|p415|||||||||
12187|Moolayember Formation|35426|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
12187|Moolayember Formation|35457|6|Mentioned|p633|||Also Fig.4 biostratigraphic relationships||||||
12187|Moolayember Formation|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
12187|Moolayember Formation|35560|4|Described|p288|||||||||
12187|Moolayember Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
12187|Moolayember Formation|35873|6|Mentioned|p16|||||||||
12187|Moolayember Formation|35901|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|36103|6|Mentioned|Table 4|||||||||
12187|Moolayember Formation|36233|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|36243|6|Mentioned|p74|||See also Table 3A.||||||
12187|Moolayember Formation|36570|6|Mentioned|p22|||||||||
12187|Moolayember Formation|36899|6|Mentioned|p1085|||||||||
12187|Moolayember Formation|36914|6|Mentioned|p87|||||||||
12187|Moolayember Formation|36921|6|Mentioned|p175|||See also Table 1.||||||
12187|Moolayember Formation|37065|5|Briefly described|p36|||||||||
12187|Moolayember Formation|37070|5|Briefly described|p70|||||||||
12187|Moolayember Formation|37075|5|Briefly described|Table 1|||||||||
12187|Moolayember Formation|37078|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|37108|6|Mentioned|p282|||||||||
12187|Moolayember Formation|37288|6|Mentioned|p41|||||||||
12187|Moolayember Formation|37451|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|37610|6|Mentioned|p302|||See also Fig.3.||||||
12187|Moolayember Formation|37612|6|Mentioned|Fig.1|||See also Fig.3.||||||
12187|Moolayember Formation|37705|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|37749|6|Mentioned|p186|||||||||
12187|Moolayember Formation|37755|6|Mentioned|p79|||||||||
12187|Moolayember Formation|37757|6|Mentioned|p29|||||||||
12187|Moolayember Formation|37996|6|Mentioned|p77|||||||||
12187|Moolayember Formation|38306|6|Mentioned|p509|||||||||
12187|Moolayember Formation|38358|4|Described|p1|||||||||
12187|Moolayember Formation|38518|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|39212|4|Described|p15|||||||||
12187|Moolayember Formation|39217|6|Mentioned|p50|||Refers Evans(1966). Miospores P51||||||
12187|Moolayember Formation|39252|6|Mentioned|p26|||||||||
12187|Moolayember Formation|39261|6|Mentioned|Fig. 9|||||||||
12187|Moolayember Formation|39275|6|Mentioned|p332|||||||||
12187|Moolayember Formation|39298|6|Mentioned|p255|||||||||
12187|Moolayember Formation|39445|5|Briefly described|Table 9|||||||||
12187|Moolayember Formation|39478|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|39491|4|Described|p23|||||||||
12187|Moolayember Formation|39494|6|Mentioned|p129|||||||||
12187|Moolayember Formation|39757|6|Mentioned|p1601|||||||||
12187|Moolayember Formation|39815|6|Mentioned|p445|||||||||
12187|Moolayember Formation|39943|6|Mentioned|Table 5A|||||||||
12187|Moolayember Formation|40030|6|Mentioned|p135|||||||||
12187|Moolayember Formation|40095|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|40120|4|Described|p428|||||||||
12187|Moolayember Formation|40123|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|40245|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|40249|6|Mentioned|p38|||||||||
12187|Moolayember Formation|40250|4|Described|p30|||||||||
12187|Moolayember Formation|40375|6|Mentioned|p133|||||||||
12187|Moolayember Formation|40539|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|40541|3|Fully described|p108|||||||||
12187|Moolayember Formation|40544|6|Mentioned|p157|||||||||
12187|Moolayember Formation|40574|6|Mentioned|p5|||||||||
12187|Moolayember Formation|40623|5|Briefly described|p80|||||||||
12187|Moolayember Formation|40634|6|Mentioned|p32|||||||||
12187|Moolayember Formation|40675|6|Mentioned|p306|||Mention Table 5A||||||
12187|Moolayember Formation|40687|6|Mentioned|Table 3|||||||||
12187|Moolayember Formation|40767|4|Described|p14|||||||||
12187|Moolayember Formation|40789|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|40832|3|Fully described|p450|||||||||
12187|Moolayember Formation|40999|6|Mentioned|p303|||||||||
12187|Moolayember Formation|41059|6|Mentioned|p168|||||||||
12187|Moolayember Formation|41097|6|Mentioned|p165|||||||||
12187|Moolayember Formation|41116|4|Described|p433|||||||||
12187|Moolayember Formation|41188|6|Mentioned|p231|||||||||
12187|Moolayember Formation|41191|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|41198|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|41210|3|Fully described|p157|||||||||
12187|Moolayember Formation|41211|6|Mentioned|p176|||||||||
12187|Moolayember Formation|41246|6|Mentioned|Map legend|Triassic||||||||
12187|Moolayember Formation|41247|6|Mentioned|p127|||See also Fig.7||||||
12187|Moolayember Formation|41266|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|41330|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|41535|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41605|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41707|6|Mentioned|p166|||||||||
12187|Moolayember Formation|41710|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41712|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|41725|6|Mentioned|p403|||||||||
12187|Moolayember Formation|42061|6|Mentioned|p150|||||||||
12187|Moolayember Formation|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
12187|Moolayember Formation|42249|6|Mentioned|p23|||||||||
12187|Moolayember Formation|42447|6|Mentioned|p7|||||||||
12187|Moolayember Formation|42463|5|Briefly described|p176|||Bowen Basin||||||
12187|Moolayember Formation|42492|5|Briefly described|Table 2 P14|||||||||
12187|Moolayember Formation|42634|5|Briefly described|Table 2 P10|||||||||
12187|Moolayember Formation|42648|6|Mentioned|p41|||||||||
12187|Moolayember Formation|42701|5|Briefly described|p74|||||||||
12187|Moolayember Formation|42865|6|Mentioned|p18|||||||||
12187|Moolayember Formation|42911|5|Briefly described|p11|||||||||
12187|Moolayember Formation|42932|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|42999|5|Briefly described|Table 1,p90||Middle Triassic|||||||
12187|Moolayember Formation|43000|5|Briefly described|p108|||see also Fig.5,p112||||||
12187|Moolayember Formation|43072|5|Briefly described|p55|||||||||
12187|Moolayember Formation|43084|6|Mentioned|p16|||||||||
12187|Moolayember Formation|43105|5|Briefly described|p13|||||||||
12187|Moolayember Formation|43185|5|Briefly described|6||Triassic|||||||
12187|Moolayember Formation|43483|6|Mentioned|14||Triassic|||||||
12187|Moolayember Formation|43546|14|Not recorded|p123,p125|||||||||
12187|Moolayember Formation|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
12187|Moolayember Formation|43851|14|Not recorded|Tb p106,110,113|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
12187|Moolayember Formation|43920|14|Not recorded|p74|||||||||
12187|Moolayember Formation|43922|14|Not recorded|p326|||"The available evidence...suggests a late Lower Triassic or Middle Triassic age."||||||
12187|Moolayember Formation|43923|4|Described|p1-2||Triassic|||||||
12187|Moolayember Formation|43977|14|Not recorded|p576|||||||||
12187|Moolayember Formation|43982|14|Not recorded|Map Legend|||||||||
12187|Moolayember Formation|43987|14|Not recorded|p270,271,275,278|||||||||
12187|Moolayember Formation|43988|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|43989|14|Not recorded|Map Legend|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|43990|14|Not recorded|Map Legend||Triassic|Part of Mimosa Group||||||
12187|Moolayember Formation|43994|14|Not recorded|Map Legend|||||||||
12187|Moolayember Formation|43996|14|Not recorded|p88|||||||||
12187|Moolayember Formation|43997|14|Not recorded|p113|||||||||
12187|Moolayember Formation|43998|4|Described|p13,17,map||Triassic|||||||
12187|Moolayember Formation|44007|14|Not recorded|p49,51|||||||||
12187|Moolayember Formation|44022|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|44023|4|Described|Tb.3,p10||Triassic|||||||
12187|Moolayember Formation|44068|14|Not recorded|p17|||||||||
12187|Moolayember Formation|44091|14|Not recorded|p53,54||Triassic|||||||
12187|Moolayember Formation|44095|14|Not recorded|p283-286|||||||||
12187|Moolayember Formation|44103|14|Not recorded|p215|||||||||
12187|Moolayember Formation|44115|14|Not recorded|p17-20|||||||||
12187|Moolayember Formation|44116|14|Not recorded|p24,28|||||||||
12187|Moolayember Formation|44118|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|44124|14|Not recorded|p4|||||||||
12187|Moolayember Formation|44129|14|Not recorded|p95-96||Triassic|||||||
12187|Moolayember Formation|44130|14|Not recorded|p280-283|||||||||
12187|Moolayember Formation|44133|6|Mentioned|p86|||Of the Galilee and Bowan Basins.||||||
12187|Moolayember Formation|44166|14|Not recorded|p8|||||||||
12187|Moolayember Formation|44169|2|Defined|Tb.1,6,8,9,12,map|||||||||
12187|Moolayember Formation|44170|2|Defined|p1,17,19-22,25,31,||Triassic|24-40,57,Pl.1,Tb.1,map||||||
12187|Moolayember Formation|44172|14|Not recorded|p1339|||||||||
12187|Moolayember Formation|44207|14|Not recorded|p115|||||||||
12187|Moolayember Formation|44243|14|Not recorded|p649,map||Triassic|||||||
12187|Moolayember Formation|44245|5|Briefly described|Map Legend||Triassic|||||||
12187|Moolayember Formation|44337|5|Briefly described|Map Legend||Triassic|Lithology.||||||
12187|Moolayember Formation|44381|14|Not recorded|p7|||||||||
12187|Moolayember Formation|44390|14|Not recorded|p6,8,14,Tb.1|Late Triassic|Middle Triassic|Of Mimosa Group.||||||
12187|Moolayember Formation|44391|14|Not recorded|Map Legend|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|44414|14|Not recorded|p114,-115|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|44419|14|Not recorded|p274||Triassic|||||||
12187|Moolayember Formation|44420|14|Not recorded|p2,3,6,7,9,12-19,21,|||p22,24,Figs.14,15.||||||
12187|Moolayember Formation|44421|14|Not recorded|p6,9,10,13,15,18,19||Triassic|||||||
12187|Moolayember Formation|44422|14|Not recorded|p150,152,153|||(Middle-Late Triassic or Early Jurassic)||||||
12187|Moolayember Formation|44423|14|Not recorded|p21-22|||||||||
12187|Moolayember Formation|44426|14|Not recorded|p12||Triassic|Triassic, from macro and microfaunas.||||||
12187|Moolayember Formation|44573|14|Not recorded|p97||Triassic|||||||
12187|Moolayember Formation|44607|14|Not recorded|p35,36|||||||||
12187|Moolayember Formation|44608|14|Not recorded|p19||Jurassic|||||||
12187|Moolayember Formation|44610|14|Not recorded|p49,Tb.1|||||||||
12187|Moolayember Formation|44636|14|Not recorded|p164||Triassic|||||||
12187|Moolayember Formation|44640|14|Not recorded|p31|||||||||
12187|Moolayember Formation|44652|14|Not recorded|p70,73,74|||||||||
12187|Moolayember Formation|44668|14|Not recorded|p59,60|||||||||
12187|Moolayember Formation|44787|14|Not recorded|Tb.p12,124,diag.p126||Late Triassic|||||||
12187|Moolayember Formation|44892|14|Not recorded|p30|||||||||
12187|Moolayember Formation|45071|3|Fully described|p75|||On Table 14||||||
12187|Moolayember Formation|45073|6|Mentioned|p59|||Strat. table||||||
12187|Moolayember Formation|45095|6|Mentioned|p18|||Refers Malone et al. (1969)||||||
12187|Moolayember Formation|45110|3|Fully described|Table 17|||See also Fig.5.||||||
12187|Moolayember Formation|46881|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
12187|Moolayember Formation|46989|5|Briefly described|Table 1|||||||||
12187|Moolayember Formation|48585|4|Described|p1,7,8,10,14,15,Pl.1|||||||||
12187|Moolayember Formation|48600|14|Not recorded|p13,20|||Springsure area.||||||
12187|Moolayember Formation|48606|14|Not recorded|p5,6,14,22|||(H/55-8 ; G55-12). Pl.1 sh.2.||||||
12187|Moolayember Formation|48611|4|Described|p7-9,12,16|||||||||
12187|Moolayember Formation|48626|14|Not recorded|Fig.1||Triassic|||||||
12187|Moolayember Formation|48898|6|Mentioned|p54|||Triassic||||||
12187|Moolayember Formation|48900|3|Fully described|p45|||Triassic.||||||
12187|Moolayember Formation|48919|2|Defined|p33|Late Triassic|Middle Triassic|See also P34-35. Middle - Upper Triassic.M - U||||||
12187|Moolayember Formation|48920|3|Fully described|p35|||Triassic||||||
12187|Moolayember Formation|48951|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|48995|6|Mentioned|p24|||||||||
12187|Moolayember Formation|61076|5|Briefly described|p188 Fig. 2|Triassic|Triassic|Age: <240Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
12187|Moolayember Formation|61313|6|Mentioned|p104 Table G1|||||||||
12187|Moolayember Formation|61377|5|Briefly described|p151|Middle Triassic|Middle Triassic|Consists of marine + non-marine interbedded sandstone, siltstone, shale and coal. A major hydrocarbon reservoir on western side of Surat Basin. Conformably overlies the Snake Creek Mudstone Member. Geol.Prov: Surat Basin. See also p139, p149 Fig. SU8.||||||07-FEB-11
12187|Moolayember Formation|61612|6|Mentioned|p276, p277, p270 Fig. 1|Middle Triassic|Middle Triassic|Includes Snake Creek Mudstone Member. Geological Province: Bowen Basin.  QLD.||||||17-MAR-09
12187|Moolayember Formation|61782|5|Briefly described|p281, p282|Middle Triassic|Middle Triassic|Geological Province: Taroom Trough. Alluvial and lacustrine sediments.||||||
12187|Moolayember Formation|62357|5|Briefly described|p524 Fig. 7, p528|Middle Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
12187|Moolayember Formation|63172|6|Mentioned|p329|||Includes microfloras in both upper and lower sequences. In the Mimosa Syncline.||||||07-FEB-11
12187|Moolayember Formation|63713|5|Briefly described|p1507 Fig.2|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Clematis Group and Warang Sandstone.||
12187|Moolayember Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Clematis Group.||
12187|Moolayember Formation|64856|3|Fully described|p41-42, p46, p51, p70, p72-79, p102|Middle Triassic|Middle Triassic|Originally the Moolayember Shale of Reeves (1947). Renamed as Moolayember Formation by Phillips (1960) and defined by Mollan et al. (1972). Bowen Basin, Galilee Basin. Datum for the top of the Triassic. Interbedded mudstones and sandstones. Contains Snake Creek Mudstone Member. Overlies Showgrounds Sandstone conformably and Arbroath beds unconformably. Unconformably overlain by Precipice Sandstone. Age from palynoflora (units APT31-34). Thickness <736m.|| ||||29-NOV-17
12187|Moolayember Formation|64857|4|Described|p126-127, 128-129, p113 Fig.3|Triassic|Triassic|Bowen Basin. Overlies Clematis Group. Contains the Snake Creek Mudstone Member at its base, which grades up into the upper part of the formation. Upper part divided into two informal subunits which are distinguishable in seismic reflection data.||||||
12187|Moolayember Formation|64858|6|Mentioned|p180 Fig.2, p181 Tb. 1, p182 Fig.3, p183|Middle Triassic|Middle Triassic|Bowen Basin.||||||30-NOV-09
12187|Moolayember Formation|64859|5|Briefly described|p222-4, 225, 226, 193, 195, 196, 199|Triassic|Triassic|Includes Snake Creek Mudstone Member. Potential oil, condensate and gas source rock, but mostly immature.||||||
12187|Moolayember Formation|65003|5|Briefly described|p6|||Of Bowen Basin.||||Overlies the Rewan Formation. (Overlies the Clematis Group?).|Sandstone.|30-MAR-12
12187|Moolayember Formation|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Middle Triassic|Overlies Clematis Group. Unit in the Bowen Basin.||||||14-SEP-09
12187|Moolayember Formation|65113|5|Briefly described|p347, Fig 4 p340|Middle Triassic|Middle Triassic|lithic sandstones, overlies the Clematis Group. Depositonal environment was a meandering river system.||||||
12187|Moolayember Formation|65114|5|Briefly described|p385 Fig.3, p383|Middle Triassic||Shown as Middle Triassic in the Fig.3 correlation chart but referred to as Early Triassic in the text; youngest unit in the Bowen Basin; upper part of Supersequence I||||||06-APR-10
12187|Moolayember Formation|65115|5|Briefly described|p425-426, 427, Fig 2 p403, Fig 14 p421|Late Triassic|Late Triassic|Overlies the Clematis Group and Showgrounds Sandstone in the Bowen Basin. Part of Supersequence I.||||||
12187|Moolayember Formation|65116|5|Briefly described|p451, Fig 2 p436|Middle Triassic|Middle Triassic|Overlies the Clematis Group and Showgrounds Sandstone in the Bowen Basin.||||||
12187|Moolayember Formation|65118|6|Mentioned|p493, Fig 2 p479|Middle Triassic|Middle Triassic|Overlies the Clematis Group in the Denison Trough and the Showgrounds Sandstone in the Taroom Trough, Bowen Basin.Youngest unit of the Bowen Basin.||||||06-MAR-12
12187|Moolayember Formation|65119|5|Briefly described|Table 1, Figs 6-8, 11-12 ,14, 16-19|Middle Triassic|Middle Triassic|Bowen Basin.  Mudstone, lithic sandstone, carbonaceous shale, conglomerate. Alluvial and lacustrine deposition up to 1650 m thick. Age: 231-240 Ma. Fission Track age: 105-183 Ma. See also misspelling Moolyember Formation p503.||||||07-MAR-12
12187|Moolayember Formation|65489|5|Briefly described|p144 Fig.53|Middle Triassic|Middle Triassic|Galilee Basin.||||Overlies Warang Sandstone and Clematis Formation.||
12187|Moolayember Formation|66188|6|Mentioned|441, 450, Fig 3, TB1, Fig 16-17|Middle Triassic|Late Permian|Of the Eromanga Basin, providing an upper age on the Galilee Basin deformation.||||||
12187|Moolayember Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Clematis Sandstone. Is unconformably overlain by Hutton, Blantyre and Precipice Sandstones.||
12187|Moolayember Formation|66615|6|Mentioned|p2 Fig.1, p2-4, p4 Fig.2, p5 Fig.3, p6-8|Triassic|Triassic|Green (1997). Age determined from palynological evidence. Denison and Southern Taroom Trough, Bowen Basin. Makes up most of subcrop beneath the Surat Basin. Known in company nomenclature as Wandoan Formation.|||Includes Snake Creek Mudstone Member.|Overlies Clematis Group.||
12187|Moolayember Formation|67133|5|Briefly described|p2, p5, p9, p19-21|Middle Triassic|Middle Triassic|Two samples of this unit were analysed by XRD and optical microscopy for this study. Both contained illite-rich mixed-layers. Fluvial deposits in an internally drained basin.||||Overlies Clematis Group. Is overlain by Precipice Sandstone.|Interbedded mudstones and coarse-grained lithic sandstones.|
12187|Moolayember Formation|67323|5|Briefly described|p81, p84, p92, p93 Fig.12.3|Triassic|Triassic|Galilee Basin.||||Conformably overlies Warang Sandstone. Is overlain by Hutton Sandstone.|Includes siltstone and carbonaceous coaly material.|
12187|Moolayember Formation|67402|4|Described|p18 fig WSD2|Ladinian|Anisian|Bowen Basin. Regional hydrocarbon (gas) or carbon dioxide storage seal. Deposited in a fluvial to lacustrine environment. Generally more than 100m thick. See also p19 fig WSD3, WSD4, p129 fig GLL9, p131 fig GLL12, p132, p133, p134, p147 fig SRT5, p21, p30, p30 fig PSA7, p31 fig PSA8, PSA9, p45, p48, p50 fig BWS4, p52, p53, p55-p57, p59, p62, p72, p80, p82 fig BWN4, p85 tbl BWN2, p124 fig GLL1, p125 tbl GLL1, p127 fig GLL5, p128 fig GLL8, p129, p135-138, p165 tbl LPB1, p300.||||Overlain by the Precipice Sandstone. Overlies the Snake Creek Mudstone, Warang Sandstone and Clematis Sandstone.|Coarsening upwards succession of mudstone, siltstone and volcanolithic sandstones.|
12187|Moolayember Formation|67669|5|Briefly described|p11|Middle Triassic|Middle Triassic|Of Bowen Basin.||Unit of Mimosa Group.||Overlain by Precipice Sandstone. Underlain by Clematis Formation. Laterally grades into Wandoan Sandstone.||
12187|Moolayember Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Overlies Clematis Group. Is unconformably overlain by Precipice Sandstone.||
12187|Moolayember Formation|68004|5|Briefly described|p172.|Middle Triassic|Middle Triassic|Petroleum-producing. Low reservoir potential because of extensive silicification and alteration of clays. Acts as a regional seal.||||||
12187|Moolayember Formation|68279|5|Briefly described|p1-4, p5 Tb.2, p7, p13-19|Ladinian|Anisian|Galilee Basin. A potential seal to the Clematis Group, a carbon geostorage target reservoir. Mineralogy of 104 samples was grouped into five major types which are described in some detail. Deposited by low-energy westerly-flowing fluvial systems. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Conformably overlies Clematis Group.||
12187|Moolayember Formation|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably underlain by the Clematis Group.|Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|68413|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably underlain by the Warang Sandstone.|Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin.||||Conformably overlies Clematis Group.||
12187|Moolayember Formation|68576|4|Described|Q_4: p1,p3,p7,p12, p14-15, p17, p21, p24|Middle Triassic|Middle Triassic|Youngest unit in the Bowen Basin. The overlying unconformity represents a 40 m.y. hiatus and separates the Bowen Basin from the Surat Basin. Sediments sourced from a volcanic province to the E. Mainly fine-grained sediments which weather to a flat terrain with no outcrops. Deposition in a dominantly fluvial-lacustrine environment; locally abundant acritarchs in the upper part indicate at least brackish conditions occasionally.|||Snake Creek Mudstone Member.|Overlies Clematis Group. Is unconformably overlain by the Precipice Sandstone.|Dominantly interbedded olive, green-brown and green-grey mudstones and lithic to sub-labile, medium- to coarse-grained sandstones. Lesser grey to black carbonaceous shale, siltstone, mudstone, coal, conglomerate; minor tuff and limestone.|
12187|Moolayember Formation|68679|5|Briefly described|p353, p364, p376-377, p381, p383-384|Triassic|Triassic|See also p391, p397, p469-470. Mollan et al. (1972); Dickins and Malone (1973). Connors-Auburn Province. Youngest unit in the Bowen Basin. Sediment was sourced from the east. 736m thick. Enclosed fluvial deposits with marginal alluvial fans, meandering streams and lakes. Minor gas producer.|||Snake Creek Mudstone Member.|Overlies the Clematis Group and the Showgrounds Sandstone.|Interbedded olive and greenish mudstone and lithic to sublabile, medium- to coarse-grained sandstone; grey to black carbonaceous shale, siltstone, mudstone, conglomerate.|
12187|Moolayember Formation|68731|5|Briefly described|p198, p201, pp200-201 Fig 3.110|Middle Triassic|Middle Triassic|Bowen Basin. Largely equivalent to the upper Warang Sandstone, but, in the Lovelle Depression this uppermost unit overlies the Warang Sandstone.||||Underlain by the Warang Sandstone.||
12187|Moolayember Formation|68901|6|Mentioned|p2 Fig. i|Triassic|Triassic|||||||27-SEP-18
12187|Moolayember Formation|69582|5|Briefly described|p35, p38, p65|||Surat Basin.||||Overlies the Showgrounds Sandstone and the Clematis Sandstone.|Sandstone.|
12187|Moolayember Formation|69591|6|Mentioned|p100|Middle Triassic|Middle Triassic|Bowen Basin. Mentioned as being age-equivalent to redbeds from boreholes drilled into the Canobie Depression, ~40km N of Cloncurry.||||||
12187|Moolayember Formation|69594|6|Mentioned|p534, p535 Fig.7.16|||||||Is overlain unconformably by Eddystone beds and Precipice Sandstone.||
12187|Moolayember Formation|69681|6|Mentioned|p82|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
12187|Moolayember Formation|69952|6|Mentioned|p85|Triassic|Triassic|||||||
12187|Moolayember Formation|70821|5|Briefly described|p80|||Basement to Eromanga, Surat Basins.||||Is overlain unconformably by Precipice Sandstone.||14-DEC-16
12187|Moolayember Formation|71264|6|Mentioned|p581 Fig.4|Triassic|Triassic|Bowen Basin.||||||
12187|Moolayember Formation|71265|6|Mentioned|p590|Triassic|Triassic|S Galilee Basin.||||||
12187|Moolayember Formation|71710|5|Briefly described|p370, p383, p384, p385 Fig 21, p387|Middle Triassic|Middle Triassic|Geological province: Galilee Basin. Overfill basin phase associated with thrust loading.||sequence 10.||Underlain, gradationally in places, by Clematis Group; locally underlain by Warang Sandstone?|Predominantly multicoloured lutites with labile sandstone and subordinate quartzose sandstone.|
12187|Moolayember Formation|71805|5|Briefly described|p80|Triassic|Triassic|Cored in Woleebee Creek GW4. Wireline logs exist for the core and for this unit.||||Overlain by the Precipice Sandstone.||
12187|Moolayember Formation|72088|4|Described|p6, p8, p15, p17, p21, p23, p91|Ladinian|Anisian|Galilee and Bowen basins. The thickest and most widespread unit across the entire basin. Deposited in a fluvio-lacustrine environment. Partly laterally equivalent to the Warang Sandstone. Compositionally very similar to the Clematis Group, although it is generally much finer grained, moderately to poorly sorted and with numerous sub-angular grains. Hosts calcite and siderite veins,||||Conformably overlies the Clematis Group and the Warang Sandstone.|Green, grey, brown, purple and red mudstone with minor siltstone and some pebbly sandstone.|
12187|Moolayember Formation|72297|5|Briefly described|p697, p744-745|Middle Triassic|Middle Triassic|Bowen Basin. A potential regional seal.|||Snake Creek Mudstone Member.||Includes minor coal.|
12187|Moolayember Formation|72298|5|Briefly described|p801|Jurassic|Triassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||||Overlies Clematis Sandstone. Is overlain unconformably by Hutton or Precipice Sandstones.||
12187|Moolayember Formation|73037|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|73038|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|73113|5|Briefly described|p. 22-24, 31, 37, 41, 46, 49, 88, 98...|||Bowen Basin. Tight aquitard. More locations: p. 115-116, 119, 146, 151-153, 169-172, 177, 179, 191.||||Underlain by Clematis Sandstone. Unconformably overlain by Precipice Sandstone.||
12187|Moolayember Formation|73246|6|Mentioned|p190|Middle Triassic|Middle Triassic|Bowen Basin, northeast and northwest. Misspelt as Moolyamber Formation p190 Fig.2.||||Underlain by Clematis Group.||30-MAR-23
12187|Moolayember Formation|73304|6|Mentioned|p76|||||||||
12187|Moolayember Formation|73306|5|Briefly described|p565|||Bowen Basin.||||Correlated with Toogoolawah Group.||
12187|Moolayember Formation|73472|4|Described|p115-116, p120, p123, p125, p130-131|Carnian|Ladinian|Galilee Basin and Bowen Basin. Maximum thickness of ca 150 m. Fluvio-lacustrine depositional setting. [See article for palynology]. An age range of 240-231 Ma was suggested based on apatite fission-track dating.|240-231 Ma|||Underlain by and interfingers with the Warang Sandstone. Underlain by Clematis Sandstone and Clematis Group. Equivalent to Warang Sandstone.|Predominantly reddish-brown claystone and light greyish siltstone with less abundant light greyish medium- to coarse-grained cross-bedded sandstones in fining-upwards intervals.|
12187|Moolayember Formation|73600|5|Briefly described|p192, p198-200, p203-204|Middle Triassic|Middle Triassic|Bowen Basin, topmost unit. Deposited in a fast-subsiding foreland setting. Believed to be derived entirely from the New England Orogen, despite no published detrital geochronology. May be recycled into the Eddystone Beds of the overlying Surat Basin, meaning that the two may be difficult to distinguish from one another.||||Unconformably overlain by the Precipice Sandstone.||
12236|Moondarra Siltstone|22453|6|Mentioned|p 11  Fig 10|||||||||
12236|Moondarra Siltstone|23396|5|Briefly described|p422|Statherian|Statherian|1668+/-8Ma||||||
12236|Moondarra Siltstone|23397|5|Briefly described|p467 Fig.5|Statherian|Statherian|1668+/-8Ma||||||
12236|Moondarra Siltstone|23398|5|Briefly described|p454||Statherian|Of Mount Isa Group. Age: 1668+/-8Ma (max.).||||||02-APR-07
12236|Moondarra Siltstone|23399|4|Described|p489|Statherian|Statherian|Of the Mount Isa Group. Age: 1668+/-8Ma.||||||02-APR-07
12236|Moondarra Siltstone|23408|5|Briefly described|p511, p513 Fig. 2|||Of Mount Isa Group.||||||15-JUN-09
12236|Moondarra Siltstone|23466|5|Briefly described|p267|Statherian|Statherian|Age: 1668+/-8Ma.||||||02-APR-07
12236|Moondarra Siltstone|23518|4|Described|p12|Proterozoic|Proterozoic|Of Mount Isa Group.  Geological Province: Western Fold Belt.||||||
12236|Moondarra Siltstone|23969|6|Mentioned|p1372 Fig.3a|||Geological Province: Mount Isa Inlier. Of the Mount Isa Group||||||02-MAR-05
12236|Moondarra Siltstone|24308|5|Briefly described|p993, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Mount Isa Group.||||||07-NOV-08
12236|Moondarra Siltstone|24419|5|Briefly described|p18, p17|Paleoproterozoic|Paleoproterozoic|Thinly laminated, weakly micaceous siltstone, laminated siltstone, fine sandstone and dolomite, overlain by dolomitic sandstone and micaceous slate (intensely cleaved siltstone and shale). Part of the Gun Supersequence.||||||07-NOV-08
12236|Moondarra Siltstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Mount Isa Group. Overlain by Breakaway Shale. Age: 1668 Ma.  Geological Province: Leichardt River Fault Trough.||||||
12236|Moondarra Siltstone|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group.  Overlies the Warrina Park Quartzite.||||||25-AUG-04
12236|Moondarra Siltstone|30535|6|Mentioned|p405|||See also p403. Refers Bennett(1965). Type section included.||||||02-APR-07
12236|Moondarra Siltstone|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12236|Moondarra Siltstone|32041|4|Described|p355|||||||||
12236|Moondarra Siltstone|32042|5|Briefly described|p39|||||||||
12236|Moondarra Siltstone|32660|5|Briefly described|Table 5|||||||||
12236|Moondarra Siltstone|32959|6|Mentioned|Fig.21|||||||||
12236|Moondarra Siltstone|33900|5|Briefly described|p13|||||||||
12236|Moondarra Siltstone|34499|6|Mentioned|Table 1|||||||||
12236|Moondarra Siltstone|35074|6|Mentioned|Fig.2|||||||||
12236|Moondarra Siltstone|35116|6|Mentioned|p181|||||||||
12236|Moondarra Siltstone|35932|6|Mentioned|p461|||||||||
12236|Moondarra Siltstone|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|36637|6|Mentioned|p1242|||||||||
12236|Moondarra Siltstone|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12236|Moondarra Siltstone|37568|5|Briefly described|p84|||||||||
12236|Moondarra Siltstone|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|38232|6|Mentioned|p89|||||||||
12236|Moondarra Siltstone|38276|6|Mentioned|p166|||||||||
12236|Moondarra Siltstone|38348|6|Mentioned|p9|||||||||
12236|Moondarra Siltstone|38350|4|Described|p15|||||||||
12236|Moondarra Siltstone|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mount Isa Group.  Overlies the Warrina Park Quartzite; underlies the Breakaway Shale.||||||25-AUG-04
12236|Moondarra Siltstone|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12236|Moondarra Siltstone|39445|5|Briefly described|Table 2|||||||||
12236|Moondarra Siltstone|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|39561|6|Mentioned|Fig.8|||||||||
12236|Moondarra Siltstone|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group. Cream to red-brown laminated siltstone, fine sandstone, dolomitic siltstone and dolomite.||||||15-JUN-06
12236|Moondarra Siltstone|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12236|Moondarra Siltstone|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12236|Moondarra Siltstone|40202|6|Mentioned|p722|||||||||
12236|Moondarra Siltstone|40221|4|Described|p19|||||||||
12236|Moondarra Siltstone|40598|6|Mentioned|p32|||||||||
12236|Moondarra Siltstone|40623|5|Briefly described|p95|||||||||
12236|Moondarra Siltstone|41248|6|Mentioned|Fig.2|||||||||
12236|Moondarra Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
12236|Moondarra Siltstone|41307|4|Described|p15|||||||||
12236|Moondarra Siltstone|42350|6|Mentioned|Fig.1 P543|||||||||
12236|Moondarra Siltstone|42782|6|Mentioned|p458|||of Mount Isa Group||||||
12236|Moondarra Siltstone|43616|6|Mentioned|p3|||||||||
12236|Moondarra Siltstone|44517|2|Defined|p234,235,map||Paleoproterozoic|Unit of Mount Isa Group.||||||07-NOV-08
12236|Moondarra Siltstone|45072|6|Mentioned|p8|||Mount Isa Group||||||
12236|Moondarra Siltstone|45136|3|Fully described|p24|||||||||
12236|Moondarra Siltstone|45161|5|Briefly described|Table 8|||||||||
12236|Moondarra Siltstone|45166|5|Briefly described|p28|||||||||
12236|Moondarra Siltstone|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
12236|Moondarra Siltstone|47083|5|Briefly described|p18|||Equivalent to Gunpowder Creek Formation. Of Mount Isa Group.||||||
12236|Moondarra Siltstone|49041|6|Mentioned|Table 4|||||||||
12236|Moondarra Siltstone|50100|5|Briefly described|p19|Statherian|Statherian|Of the Mount Isa Group.  Thinly laminated, weakly micaceous siltstone, laminated siltstone, fine sandstone and dolomite, overlain by dolomitic sandstone and micaceous slate.  Geological Province: Western Fold Belt Province.||||||
12236|Moondarra Siltstone|50332|5|Briefly described|p21, p95|Proterozoic|Proterozoic|Of the Mount Isa Group. Overlain comformably by Breakaway Shale. Geological Province: Western Fold Belt Province. Consists of micaceous and laminated siltstones, dolomitic sandstone and micaceous slate.||||||07-FEB-11
12236|Moondarra Siltstone|50550|6|Mentioned|p1141 Fig.4||Statherian|Of Mount Isa Group. Geological Province: Western Fold Belt.||||||19-DEC-07
12236|Moondarra Siltstone|50624|5|Briefly described|p237 Fig.4||Statherian|Of the Mount Isa Group.||||||02-APR-07
12236|Moondarra Siltstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Isa Group. Dolomitic, pyritic siltstone, limestone, dolomite.||||||
12236|Moondarra Siltstone|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Includes Warrina Park Quartzite. Overlain by Breakaway Shale. Geological Province: Western Fold Belt.||||||03-JUN-09
12236|Moondarra Siltstone|61736|5|Briefly described|p673|Paleoproterozoic|Paleoproterozoic|Age: 1668+/-8Ma.||||||24-FEB-10
12236|Moondarra Siltstone|61923|5|Briefly described|p29 Fig.2, p30|||Of the Mount Isa Group. Finely laminated, grey siltstone interlayered with very thin, fine-grained sandstone layers. Conformably overlies Warrina Park Quartzite; overlain by Breakaway Shale. Geological Province: Mount Isa Inlier.||||||
12236|Moondarra Siltstone|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1668Ma. Geological Province: Isa Superbasin, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
12236|Moondarra Siltstone|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Mount Isa. Shown as Moondarra Slst.||Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
12236|Moondarra Siltstone|62535|5|Briefly described|p672-673|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.|<1668 +/- 8 Ma.|Mount Isa Group.||||
12236|Moondarra Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
12236|Moondarra Siltstone|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
12236|Moondarra Siltstone|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Gun supersequence.||||||
12236|Moondarra Siltstone|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Moondarra.||Of the Gun supersequence||||
12236|Moondarra Siltstone|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
12236|Moondarra Siltstone|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
12236|Moondarra Siltstone|63866|5|Briefly described|p58|Statherian|Statherian|Isa Superbasin.|1668 +/- 8 Ma  (Maximum depositional age)|Gun Supersequence||||
12236|Moondarra Siltstone|64250|6|Mentioned|p11 fig.3, p17 fig.7||||<1668 +/- 8 Ma|Unit in Mount Isa Group||||
12236|Moondarra Siltstone|65396|5|Briefly described|p82, p175, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Leichhardt River Fault Trough. Detrital zircon sources listed.|<1688 +/- 8 Ma.|Mount Isa Group||Overlain by Breakaway Shale.||04-APR-17
12236|Moondarra Siltstone|66844|5|Briefly described|p266|||Mount Isa region. See also Moondarra Formation p244.||Within Gun Supersequence; Gun 1.1 and 1.2. Of lower McNamara Group.||||
12236|Moondarra Siltstone|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
12236|Moondarra Siltstone|67323|4|Described|GIS attrib tbl, p12-13|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Isa Superbasin. Leichhardt River Domain, Mount Isa Inlier.|1668 +/- 8 Ma (maximum depositional age).|Mount Isa Group.||Time equivalent to Hero Formation|Cream to red-brown laminated siltstone, fine sandstone, dolomitic siltstone and dolomite.|
12236|Moondarra Siltstone|67499|6|Mentioned|p938|Statherian|Statherian|Age based on SHRIMP U-Pb zircon dating.|1668 +/- 8 Ma|Of Mount Isa Group?||Underlain by the Warrina Park Quartzite.||
12236|Moondarra Siltstone|68542|6|Mentioned|p6|||||||Overlies Warrina Park Quartzite, overlain by Breakaway Shale||
12236|Moondarra Siltstone|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Warrina Park Quartzite. Is overlain by Breakaway Shale.||
12236|Moondarra Siltstone|68732|5|Briefly described|p160-162, p165 Fig.3, p168 Fig.5|Statherian|Statherian|Of the Gun Supersequence. Dominated by flat rhythmites. Appears as Moodarra Slt in Fig.5. Sedimentary depositional age.|1663 +/- 3 Ma|Mount Isa Group.|||Siliciclastic sediments: dominantly sandstone-siltstone-shale laminae and thin beds (rhythmites).|01-DEC-17
12236|Moondarra Siltstone|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||Mount Isa Group||||
12236|Moondarra Siltstone|69591|4|Described|p40, p43, p45|||Kalkadoon-Leichhardt Domain. Part of Gun Supersequence. Deposited below storm base/near shore. Lithologically similar to Gunpowder Creek Formation (Mount Isa Group).|1668 +/- 8 Ma (Page et al., 2000).|Mount Isa Group.||Overlies Warrina Park Siltstone or Surprise Creek Formation.|Cream to red-brown laminated siltstone, fine sandstone, dolomitic siltstone, dolomite.|
12236|Moondarra Siltstone|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Cream to red-brown laminated siltstone, fine-grained sandstone, dolomitic siltstone and dolomite. (Separately mapped) dolomitic siltstone and dolomite.|
12236|Moondarra Siltstone|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Cream to red-brown laminated siltstone, fine-grained sandstone, dolomitic siltstone and dolomite. (Separately mapped) dolomitic siltstone and dolomite.|
12236|Moondarra Siltstone|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1688+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone.|
12236|Moondarra Siltstone|71960|4|Described|p85-87, 77, 78,82, 83, p101,102,105,106|Proterozoic|Proterozoic|950 m thick in Western Fault Zone. Also interdigitates with Warrina Park Quartzite in Paroo Range area. Hero Formation underlies and lateral equivalent with gradational contact. Floodplain or flood basin deposit. See Facies G p101.||Of Mount Isa Group.||Conformable with underlying Warrina Park Formation and overlying Breakaway Shale. Unconformable on Eastern Creek Volcanics in Western Fault Zone.|Relatively deeply weathered thin-bedded alternation of siltstone and mudstone or shale, in places dolomitic.|
12236|Moondarra Siltstone|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Hero/Western Fault Zone.||Of Mount Isa Group|||Shale, dolostone, mudstone; shale, siltstone, wave-rippled sandstone, dolomitic mudstone.|
12236|Moondarra Siltstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Underlies Breakaway Shale.||
12236|Moondarra Siltstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Underlies Breakaway Shale. Shown as unconformably overlying Torpedo Creek / Warrina Park Quartzite.||
12236|Moondarra Siltstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Isa Superbasin.||Mt Isa Group||Overlain by Breakway Shale.||
12236|Moondarra Siltstone|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Leichhardt River Domain.|1668+/-8 Ma maximum depositional age||||Carbonates.|
12242|Moonie Formation|39445|5|Briefly described|Table 14|||||||||
12242|Moonie Formation|44509|14|Not recorded|p342-343|||||||||
12242|Moonie Formation|44542|14|Not recorded|p30||Tertiary|Equivalent to Telgazli Formation.||||||
12242|Moonie Formation|61155|5|Briefly described|p19|Late Eocene|Early Eocene|Thickness: 9m. Geologial Province: eastern Surat Basin.||||||
12242|Moonie Formation|69599|5|Briefly described|p580, p584, p600-601|Oligocene|Paleocene|Isbell (1957). Crops out near the Moonie River.  <9m thick. Mainly Eocene: postdates Morney profile and predates Canaway profile.||||Correlated (at least partly) with Eyre, Glendower, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; Mueller and Moses Sandstones.|Fluvial sandstone, granule conglomerate and lesser siltstone.|
12255|Moonlight Sandstone Member|23161|4|Described|p29|Early Permian|Early Permian|||||||
12255|Moonlight Sandstone Member|36739|6|Mentioned|p13|||||||||
12255|Moonlight Sandstone Member|39267|6|Mentioned|p235|||See also P237||||||
12255|Moonlight Sandstone Member|40093|6|Mentioned|p27|||||||||
12255|Moonlight Sandstone Member|41666|6|Mentioned|p27|||||||||
12255|Moonlight Sandstone Member|42257|5|Briefly described|Table 1 P263|||||||||
12255|Moonlight Sandstone Member|42701|4|Described|p64|||||||||08-SEP-14
12255|Moonlight Sandstone Member|65388|5|Briefly described|p187-188|||Regarded as of Gebbie Formation by McClung (1973, 1981), but of overlying Blenheim Formation by Waterhouse & Jell (1983).||||||
12255|Moonlight Sandstone Member|68679|5|Briefly described|p380|Permian|Permian|Waterhouse and Jell (1983). Northern Bowen Basin. NOT the top of the Gebbie Formation. See also Moonlight Sandstone (p353) which is presented as a Formation between Gebbie and Blenheim Formations. Skolithos ichnofossil suggests shallow-marine deposition.||Basal Blenheim Formation.|||Quartzose and lithic labile sandstone, sandy siltstone, coquinite and numerous conglomeratic dropstones (not seen in the Gebbie Formation).|
12259|Moonmera Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgbm].  Altered porphyritic biotite granodiorite, breccia.||||||
12259|Moonmera Granodiorite|31659|6|Mentioned|p87|||||||||
12296|Moorooka Formation|12597|5|Briefly described|p491, |||Of Houston (1965).||Unit in Woogaroo Subgroup.||||
12296|Moorooka Formation|30302|6|Mentioned|p415|||Refers Houston(1965)||||||
12296|Moorooka Formation|30455|6|Mentioned|p7|||See also P12,21. Triassic age||||||
12296|Moorooka Formation|30458|6|Mentioned|p3|||Triassic age||||||
12296|Moorooka Formation|30460|6|Mentioned|p12|||See also P13,14,22. Triassic age||||||
12296|Moorooka Formation|30465|6|Mentioned|p4|||||||||
12296|Moorooka Formation|30466|6|Mentioned|p5|||Triassic age||||||
12296|Moorooka Formation|30470|6|Mentioned|p457|||||||||
12296|Moorooka Formation|30508|6|Mentioned|p88|||Mesozoic age. Griffith University Water Supply||||||
12296|Moorooka Formation|30785|6|Mentioned|p398|||||||||
12296|Moorooka Formation|32136|6|Mentioned|p5|||Miospores||||||
12296|Moorooka Formation|35043|6|Mentioned|p78|||||||||
12296|Moorooka Formation|35053|5|Briefly described|p35|||||||||
12296|Moorooka Formation|36825|6|Mentioned|p21|||||||||
12296|Moorooka Formation|40623|5|Briefly described|p7|||||||||
12296|Moorooka Formation|41906|6|Mentioned|p34|||||||||
12296|Moorooka Formation|42316|6|Mentioned|p7|||||||||
12296|Moorooka Formation|42893|6|Mentioned|p6|||||||||
12296|Moorooka Formation|43921|14|Not recorded|p315,317,320-323|||Massive sandstones. Microfloral assemblages(320-21)||||||
12296|Moorooka Formation|43923|6|Mentioned|p5||Triassic|||||||
12296|Moorooka Formation|44030|2|Defined|p115,122,125-135||Late Triassic|||||||
12296|Moorooka Formation|44687|2|Defined|p221-224|Late Triassic|Middle Triassic|New name. These rocks previously included in Brisbane Tuffs.||||Disconformably overlies Tingalpa Formation. Disconformably overlain by Oxley Group.||21-MAR-13
12296|Moorooka Formation|44703|14|Not recorded|Map|Late Triassic|Middle Triassic|||||||
12296|Moorooka Formation|44708|14|Not recorded|p3,5,21,34,Sh.2,3||Middle Triassic|||||||
12296|Moorooka Formation|69594|5|Briefly described|p546-547|Rhaetian|Rhaetian|Houston (1967).||||A palynostratigraphic correlative of the Nambour Formation.||
12305|Mopunga Group|9394|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological Province: Georgina Basin.||||||
12305|Mopunga Group|9694|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological Province: Georgina Basin.||||||18-NOV-04
12305|Mopunga Group|12951|5|Briefly described|p143,  fig 4|Neoproterozoic|Neoproterozoic|Georgina Basin.|||Includes Elkera Formation at top.|||
12305|Mopunga Group|22649|6|Mentioned|p 137|||In the Georgina Basin.||||||07-NOV-06
12305|Mopunga Group|33103|6|Mentioned|p23|||||||||
12305|Mopunga Group|33111|5|Briefly described|p39|||Fauna.||||||
12305|Mopunga Group|35005|5|Briefly described|p145|||||||||
12305|Mopunga Group|36473|6|Mentioned|Map legend|Cambrian|Adelaidean|Adelaidean to Cambrian||||||
12305|Mopunga Group|37462|4|Described|Table 4.IX|||||||||
12305|Mopunga Group|37929|5|Briefly described|p526|||||||||
12305|Mopunga Group|38157|6|Mentioned|Table IX|||||||||
12305|Mopunga Group|38445|6|Mentioned|p102|||||||||
12305|Mopunga Group|39210|4|Described|p51|||||||||
12305|Mopunga Group|39445|6|Mentioned|p56|||||||||
12305|Mopunga Group|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Geological Province: Georgina Basin.||||||15-NOV-05
12305|Mopunga Group|40906|4|Described|p21|||Mention Fig.9||||||
12305|Mopunga Group|41429|6|Mentioned|p247|||||||||
12305|Mopunga Group|42504|5|Briefly described|p85|||||||||
12305|Mopunga Group|42643|6|Mentioned|p21|||In the Georgina Basin||||||07-NOV-06
12305|Mopunga Group|42956|5|Briefly described|p31 Fig.4|||||||||
12305|Mopunga Group|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
12305|Mopunga Group|44233|14|Not recorded|Fig.1|Early Cambrian|Adelaidean|Adelaidean-Lower Cambrian.||||||
12305|Mopunga Group|44327|14|Not recorded|Tb.I,p.4,7,8,map||Middle Cambrian|(F53-11). Mid.Camb. Consists of Elyuah, Grant Bluff and Mount Baldwin Formations.||||||07-NOV-06
12305|Mopunga Group|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
12305|Mopunga Group|45052|4|Described|p68|||Adelaidean.||||||07-NOV-06
12305|Mopunga Group|45102|6|Mentioned|p43|||See also p45,49.||||||07-NOV-06
12305|Mopunga Group|45155|6|Mentioned|Fig.7|||||||||
12305|Mopunga Group|46957|6|Mentioned|p165|||||||||
12305|Mopunga Group|48844|2|Defined|p.1,8,20|Early Cambrian|Neoproterozoic|Pl.8. U.Proterozoic-L.Cam. Disconformably overlies Mount Cornish Formation. (F53-11).||||||07-NOV-06
12305|Mopunga Group|48901|14|Not recorded|Not recorded||Adelaidean|inc. Grant Bluff Formation, Elyuah Formation, Mount Cornish Formation, Field River Beds.||||||07-NOV-06
12305|Mopunga Group|48990|1|Redefined|p17|Adelaidean|Adelaidean|||||||
12305|Mopunga Group|60122|5|Briefly described|p12|Neoproterozoic|Neoproterozoic|Includes the Elyuah Formation, Gnalla-a-Gea Arkose and Grant Bluff Formation. Geological Province: Georgina Basin. See also p5.||||||
12305|Mopunga Group|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Includes: Elkera Formation, Grant Bluff Formation, Elyuah Formation. Geological province: Georgina Basin.||||||17-NOV-04
12305|Mopunga Group|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes the Elyuah and Grant Bluff Formations and Gnallan-a-Gea Arkose.||||||25-NOV-04
12305|Mopunga Group|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Georgina Basin.||||||
12305|Mopunga Group|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes: Elyuah Fm., Gnallan-a-Gea Arkose, Grant Bluff Fm., Central Mt. Stuart Fm., Elkera Formation and the Andagera Formation.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||11-OCT-05
12305|Mopunga Group|61732|5|Briefly described|p106|||Includes: Elyuah, Grant Bluff, Elkera and Central Mount Stuart Formations.  Geological Province: Georgina Basin.||||||07-FEB-11
12305|Mopunga Group|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin.||||||
12305|Mopunga Group|62789|6|Mentioned|p129|Neoproterozoic|Neoproterozoic|In southern Georgina Basin.||||Underlies the Mount Baldwin Formation.||28-MAR-12
12305|Mopunga Group|62790|5|Briefly described|p210|Neoproterozoic|Neoproterozoic|Southern Georgina Basin.||||Underlies the Neoproterozoic-Lower Cambrian Mount Baldwin Formation.||04-DEC-12
12305|Mopunga Group|62984|5|Briefly described|p13|Neoproterozoic III|Neoproterozoic III|Ediacaran package. Geological Province: Georgina Basin.||||||23-JAN-07
12305|Mopunga Group|63562|6|Mentioned|p344|Ediacaran|Ediacaran||||Includes Grant Bluff Formation.|||
12305|Mopunga Group|64068|3|Fully described|p224 App 1, pp49-54, p35, 55, p7|Ediacaran|Ediacaran|Intended as redefinition. Adds Andagera Formation to this Group. Redefined (Walter, 1980) to exclude the Mount Baldwin Formation.|||Includes Gnallan-a-Gea Arkose; Elyuah, Elkera, Central Mount Stuart, Andagera, and Grant Bluff Formations.|Overlies Keepera Group units disconformably. Is disconformably overlain by Shadow Group units or Thorntonia Limestone.|Siliciclastic sediments.|04-APR-12
12305|Mopunga Group|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Southern Georgina Basin.||||||
12305|Mopunga Group|64812|5|Briefly described|p237 Fig. 2|Neoproterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||07-FEB-11
12305|Mopunga Group|64813|5|Briefly described|p256 Fig. 3|Neoproeterozoic|Neoproterozoic|Geological Province: southern Georgina Basin.||||||11-FEB-09
12305|Mopunga Group|65237|5|Briefly described|p5|Late Neoproterozoic|Late Neoproterozoic|Comprises Elyuah, Grant Bluff and Elkera Formations. Max. thickness: 800m. Geological province: southern Georgina Basin. Synorogenic sediments.||||||07-FEB-11
12305|Mopunga Group|65333|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wiso Basin. Includes Central Mount Stuart Formation. Arkose, subarkose, quartz arenite and siltstone.||||||
12305|Mopunga Group|65334|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wiso Basin. Subsurface only. Includes Central Mount Stuart Formation||||||
12305|Mopunga Group|65338|6|Mentioned|pp63-67.|Ediacaran|Ediacaran||||Includes Elyuah, Grant Bluff, Elkera, Central Mount Stuart and Andagera Formations and Gnallan-a-gea Arkose.|Overlies Wonnadinna Dolostone.||
12305|Mopunga Group|65341|6|Mentioned|p2 Fig.2, p5. |Ediacaran|Ediacaran|An unconformity-bound package.|||Includes Gnallan-a-Gea Arkose, Andagera, Central Mount Stuart, Grant Bluff, Elyuah and Elkera Formations.|||
12305|Mopunga Group|66767|5|Briefly described|p58|Ediacaran|Ediacaran|Georgina Basin.|||||Largely siliciclastic post-glacial sedimentary rocks.|
12305|Mopunga Group|67148|5|Briefly described|Map legend.|Ediacaran|Ediacaran||||Includes Andagera Formation.|||
12305|Mopunga Group|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.|||Includes Elyuah, Grant Bluff and Central Mount Stuart Formations.|||
12305|Mopunga Group|67352|4|Described|v, p17-18, p44 fig 48|Ediacaran|Ediacaran||||Andagera Formation|||
12305|Mopunga Group|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
12305|Mopunga Group|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Elyuah, Grant Bluff and Central Mount Stuart Formations.|||
12305|Mopunga Group|68270|5|Briefly described|p680-681,683|Ediacaran|Ediacaran|Southern Georgina Basin.||||Underlain disconformably by Boko Formation.||
12305|Mopunga Group|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.|||Elkera, Elyuah, Grant Bluff Formations; Gnallan-a-Gea Arkose.|||12-JUL-16
12305|Mopunga Group|69443|4|Described|p28:2-3, 7, 10-12, 14, 31|Ediacaran|Ediacaran|Noakes (1956); redefined by Kruse in Dunster et al. (2007). Southern Georgina Basin. Postglacial sediments deposited following the Toomba Movement. Correlated with the Amadeus Basin succession of Gaylad Sandstone-Pertatataka Formation-Julie Formation-uppermost Inindia beds-upper Boord Formation-lower Arumbera Sandstone; also with the Mount Doreen Formation and lower Yuendumu Sandstone of the Ngalia Basin.|||Elyuah, Grant Bluff, Elkera, Andagera, Central Mount Stuart Formations; Gnallan-a-gea Arkose.|Is overlain unconformably or disconformably by Shadow Group.||12-JUL-16
12305|Mopunga Group|69673|6|Mentioned|p111, p115|Neoproterozoic|Neoproterozoic||||Includes Gnallan-a-gea Arkose, Elyuah Formation, Grant Bluff Formation, Elkera Formation, Central Mt Stuart Formation, Andagera Formation|||
12305|Mopunga Group|70951|6|Mentioned|p1080|Proterozoic|Proterozoic|Part of basement geology to the Georgina Basin. Low reflectance measured.||||||
12305|Mopunga Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Elkera Formation, Grant Bluff Formation and the Elyuah Formation.|Unconformably overlain by the Shadow Group. Disconformably overlies the Keepera Group.||
12305|Mopunga Group|72516|5|Briefly described|p12-13, p21, p85, p88-90|Ediacaran|Ediacaran|Georgina Basin. Locally intruded by quartz veins. See also p96, p135, p158, p171, p176.|||Includes the Elkera Formation, Grant Bluff Formation and Elyuah Formation,|Disconformably overlies the Keepera Group.||21-APR-22
12305|Mopunga Group|72711|6|Mentioned|p3 Fig.2.|||Shown only on p3 Fig.2. From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Georgina Basin.||||||
12308|Moranbah Coal Measures|22973|5|Briefly described|p11 Fig.2(f)|Late Permian|Late Permian|||||||
12308|Moranbah Coal Measures|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
12308|Moranbah Coal Measures|22978|6|Mentioned|p148 Fig.1|||||||||
12308|Moranbah Coal Measures|22986|5|Briefly described|p291|||||||||
12308|Moranbah Coal Measures|22988|5|Briefly described|p304|||||||||
12308|Moranbah Coal Measures|22994|5|Briefly described|p345|||||||||
12308|Moranbah Coal Measures|22996|5|Briefly described|p351|Permian|Permian|||||||
12308|Moranbah Coal Measures|22997|5|Briefly described|p369|Permian|Permian|||||||
12308|Moranbah Coal Measures|22998|5|Briefly described|p377|||||||||
12308|Moranbah Coal Measures|23000|5|Briefly described|p296|||||||||
12308|Moranbah Coal Measures|23002|6|Mentioned|p417|||||||||
12308|Moranbah Coal Measures|23034|6|Mentioned|23|||||||||
12308|Moranbah Coal Measures|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
12308|Moranbah Coal Measures|23161|4|Described|p31 table4 fig11||Late Permian|||||||
12308|Moranbah Coal Measures|23430|5|Briefly described|p515-516|||Of Blackwater Group. Bowen Basin Province.||||||
12308|Moranbah Coal Measures|23444|5|Briefly described|p183|||Of Blackwater Group.||||||17-MAR-09
12308|Moranbah Coal Measures|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Blackwater Group.  Age: ~259Ma.  Geological Province: Bowen Basin.||||||
12308|Moranbah Coal Measures|30915|6|Mentioned|p92|||Intended redefinition of Fair Hill Formation||||||
12308|Moranbah Coal Measures|31690|2|Defined|p44|Late Permian|Late Permian|Mention p35, new name.||||||08-SEP-14
12308|Moranbah Coal Measures|32839|6|Mentioned|p25|||||||||
12308|Moranbah Coal Measures|35138|6|Mentioned|p8|||||||||
12308|Moranbah Coal Measures|35266|6|Mentioned|p190|||||||||
12308|Moranbah Coal Measures|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
12308|Moranbah Coal Measures|35467|6|Mentioned|Fig.3|||Rock unit correlation north Bowen Basin. Lithology described P186.||||||
12308|Moranbah Coal Measures|35937|6|Mentioned|p619|||||||||
12308|Moranbah Coal Measures|36172|6|Mentioned|Appendix|||||||||
12308|Moranbah Coal Measures|36739|6|Mentioned|p24|||||||||
12308|Moranbah Coal Measures|37458|6|Mentioned|p441|||||||||
12308|Moranbah Coal Measures|37612|3|Fully described|p290|||See also P284||||||
12308|Moranbah Coal Measures|38518|6|Mentioned|Fig.3|||||||||
12308|Moranbah Coal Measures|38951|6|Mentioned|p408|||||||||
12308|Moranbah Coal Measures|38958|5|Briefly described|p493|||||||||
12308|Moranbah Coal Measures|39212|4|Described|p28|||See P30 ideal for open-cut. See also P13||||||
12308|Moranbah Coal Measures|39252|5|Briefly described|p20|||||||||
12308|Moranbah Coal Measures|39259|6|Mentioned|p90|||||||||
12308|Moranbah Coal Measures|39261|6|Mentioned|Fig.6|||||||||
12308|Moranbah Coal Measures|39267|6|Mentioned|p235|||See also P240||||||
12308|Moranbah Coal Measures|39268|6|Mentioned|p270|||||||||
12308|Moranbah Coal Measures|39269|5|Briefly described|p275|||Sedimentary environment||||||
12308|Moranbah Coal Measures|39274|4|Described|p317|||||||||
12308|Moranbah Coal Measures|39445|5|Briefly described|Table 8|||See also Table 9||||||
12308|Moranbah Coal Measures|40087|6|Mentioned|p242|||||||||
12308|Moranbah Coal Measures|40321|6|Mentioned|Fig.3|||||||||
12308|Moranbah Coal Measures|40749|6|Mentioned|Fig.1|||||||||
12308|Moranbah Coal Measures|41191|5|Briefly described|p283|||||||||
12308|Moranbah Coal Measures|41226|6|Mentioned|Table 1|||||||||
12308|Moranbah Coal Measures|41246|6|Mentioned|Map legend|Permian||||||||
12308|Moranbah Coal Measures|41247|6|Mentioned|Table 4|||||||||
12308|Moranbah Coal Measures|41474|6|Mentioned|p62|||||||||
12308|Moranbah Coal Measures|41689|6|Mentioned|Table 1|||||||||
12308|Moranbah Coal Measures|41921|6|Mentioned|Fig.1|||||||||
12308|Moranbah Coal Measures|42091|6|Mentioned|p289|||||||||
12308|Moranbah Coal Measures|42120|6|Mentioned|p412|||||||||
12308|Moranbah Coal Measures|42187|6|Mentioned|Fig.3 P318|||||||||
12308|Moranbah Coal Measures|42249|6|Mentioned|p23|||||||||
12308|Moranbah Coal Measures|42250|6|Mentioned|Fig.4 P31|||||||||
12308|Moranbah Coal Measures|42251|4|Described|p39|||||||||
12308|Moranbah Coal Measures|42252|5|Briefly described|p50|||||||||
12308|Moranbah Coal Measures|42256|6|Mentioned|Fig.1 P243|||||||||
12308|Moranbah Coal Measures|42257|5|Briefly described|Table 1 P263|||||||||
12308|Moranbah Coal Measures|42259|6|Mentioned|p18|||||||||
12308|Moranbah Coal Measures|42648|5|Briefly described|p40|||||||||
12308|Moranbah Coal Measures|42662|4|Described|p85|||||||||
12308|Moranbah Coal Measures|42701|4|Described|p68|||||||||
12308|Moranbah Coal Measures|42932|6|Mentioned|Table 1|||of Jensen(1975), Koppe (1978), Staines & Koppe (1980)||||||
12308|Moranbah Coal Measures|50115|5|Briefly described|p53, p55 Fig.2|Late Permian|Late Permian|Contains Goonyella Upper Middle and Lower seams. Geological Province: Bowen Basin.||||||
12308|Moranbah Coal Measures|60115|5|Briefly described|p20, p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||04-FEB-08
12308|Moranbah Coal Measures|60472|5|Briefly described|Map Legend|Late Permian - Correct|Late Permian - Correct|Of the Blackwater Group. Labile sandstone, siltstone, mudstone, coal, conglomerate.||||||
12308|Moranbah Coal Measures|60659|5|Briefly described|p21|Late Permian|Late Permian|Of Blackwater Gp. Lithic labile sandstone, siltstone, carbonaceous shale, coal, locally cherty mudstone and minor conglomerate. Fossil wood and leaf impressions occur in the siltstone and shale. Conformably overlies Exmoor Formation.||||||07-FEB-11
12308|Moranbah Coal Measures|61232|5|Briefly described|p119, p120 Fig.1, p126, Fig.4|Late Permian|Late Permian|Of the northern Bowen Basin||||Lateral equivalent of German Creek Coal Measures||
12308|Moranbah Coal Measures|61612|6|Mentioned|p272, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
12308|Moranbah Coal Measures|64665|5|Briefly described|p52, p53 Fig.2.|Middle Permian|Middle Permian|Bowen Basin. Deposited in a deltaic environment during the early stages of foreland basin development. An important coking coal-bearing unit. Low ash coal with good coking properties; high-volatile bituminous to anthracite.||||Overlies German Creek Formation. Is overlain by Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|65388|3|Fully described|p198-199, 191, 200|Lopingian|Guadalupian|Basal unit of Blackwater Group in northern Bowen Basin.  Defined: Koppe (1978). Apparently conformably overlies Exmoor Formation. Conformably overlain by Fort Cooper Coal Measures. Age from microflora: AAP5 (Price, 1997). SHRIMP U/Pb age from tuff: 258.9+/- 2.7 Ma. Type section in Grosvenor NS14 (152.4-411.1m); reference section  in Rosella Creek.||||||
12308|Moranbah Coal Measures|66086|5|Briefly described|Map legend|Permian|Permian|Unit in Blackwater Group. Conformably overlain by Fort Cooper Coal Measures. Labile sandstone, siltstone, mudstone, coal, conglomerate in the east.||||||
12308|Moranbah Coal Measures|67365|5|Briefly described|p84.|Late Permian|Middle Permian|Northern Bowen Basin. Produces CSG from horizontal in-seam wells.||||||
12308|Moranbah Coal Measures|67402|6|Mentioned|p21, p45, p80 tbl BWN1|Wuchiapingian|Wuchiapingian|Bowen Basin. See also p82, p83, p85, p165 tbl LPB1, p272, p310.||Blackwater Group||Overlies the Exmoor and Blenheim Formations. Overlain by the Rangal and Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Fort Copper Coal Measures. Underlain by German Creek Formation||
12308|Moranbah Coal Measures|67788|6|Mentioned|p22-23, 27-28|Permian|Permian|Northern Bowen Basin, QLD. Crossplot of channel belt width against thickness for channel sandstones. Alluvial to coastal plain sediments feeding marine deltas.||||||
12308|Moranbah Coal Measures|68679|5|Briefly described|p353, p377, p381-382, p384|Permian|Permian|Koppe (1978). Connors-Auburn Province. Bowen Basin. 800m thick. Delta plain sediments. Properties of the coal are described in some detail. Produces CSG.||Blackwater Group.||Overlies Exmoor Formation (conformably) and locally German Creek Formation. Is overlain by Fort Cooper Coal Measures.|Labile sandstone, siltstone, mudstone, coal.|
12308|Moranbah Coal Measures|70330|5|Briefly described|p10-12, 14-16|Late Permian|Late Permian|Bowen Basin. Formed in generally prograding alluvial to coastal environments. Appears in the text as MCM after the first couple of mentions.||Blackwater Group.||||
12308|Moranbah Coal Measures|70815|6|Mentioned|p3-5, 9|||Bowen Basin. Vitrinite reflectance values mapped.|||||Produces high-quality coking coal.|
12308|Moranbah Coal Measures|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Bowen Basin.||Unit of Tinowon Formation.|Includes Platypus Tuff.|||
12308|Moranbah Coal Measures|70861|5|Briefly described|p36-37|Late Permian|Late Permian|Of Bowen Basin.||Unit of Blackwater Group.||Overlain by Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|70940|5|Briefly described|p843-844, p846|Permian|Permian|Bowen Basin.||Blackwater Group.||Is overlain by Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|71265|5|Briefly described|p589|Changhsingian|Wuchiapingian|Bowen Basin.||||Overlie Blenheim Formation. Is overlain by Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|71276|5|Briefly described|p294-297|||Bowen Basin.|> 256 Ma (Nicoll et al., 2015).|||Passes laterally into Catherine Sandstone.||
12308|Moranbah Coal Measures|71701|5|Briefly described|p155, p159, p167, p169|Wuchiapingian|Wuchiapingian|Northern Area, Bowen Basin.|||Includes the Platypus Tuff.|Overlies the Blenheim Formation. Overlain by the Fort Cooper Coal Measures.||10-FEB-23
12308|Moranbah Coal Measures|72297|5|Briefly described|p694-695, p703, p705|Permian|Permian|Koppe (1978). NE Bowen Basin. Excellent high-grade, vitrinite-rich, hard coking coal seams. Fluvial floodplain deposits. Coal seam correlation diagram. Indicative properties of export coking and thermal coals tabulated.|||Goonyella Lower, Goonyella Middle, Goonyella Upper, Dysart Lower, Dysart Upper, Harrow Creek Lower, Harrow Creek, Seams.|Overlies German Creek Formation. Is overlain by Fair Hill, Macmillan Formations and Fort Cooper Coal Measures. Upper part is equivalent to Macmillan Formation.|Includes sub-bituminous coal.|
12308|Moranbah Coal Measures|73036|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Labile sandstone, siltstone, mudstone, coal, conglomerate in the east.|
12308|Moranbah Coal Measures|73037|5|Briefly described|Map legend|Late Permian|Late Permian|Shown as Formation rank unit.||Blackwater Group|||Labile sandstone, siltstone, mudstone, coal, conglomerate in the east.|
12308|Moranbah Coal Measures|73038|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Labile sandstone, siltstone, mudstone, coal, conglomerate in the east.|
12308|Moranbah Coal Measures|73040|5|Briefly described|Map legend|Late Permian|Late Permian|||Blackwater Group|||Labile sandstone, siltstone, mudstone, coal, conglomerate in the east.|
12308|Moranbah Coal Measures|73163|6|Mentioned|p474|Lopingian|Lopingian|Bowen Basin. Contains the P-Tuff volcanic ash layer. Ages from the P-Tuff.|258.9 +/- 2.7, 256.0 +/- 0.07 Ma||includes P-Tuff|||
12308|Moranbah Coal Measures|73246|6|Mentioned|p190-191|Upper Permian|Upper Permian|Bowen Basin, northeast and northwest.||Blackwater Group||Underlain by Back Creek Group including Exmoor and German Creek formations of Blenheim Subgroup. Overlain Fort Cooper Coal Measures. Partly equivalent to Fair Hill Formation and Blenheim Subgroup.||
12308|Moranbah Coal Measures|73305|6|Mentioned|p547, p548 Fig.1, p550, p552, p561|Late Permian|Late Permian|Bowen Basin. Collinsville Shelf and Nebo Synclinorium. Abbreviated to MCM in text.||||Underlies the Fort Cooper Coal Measures, time-equivalent to the Wallabella Coal Measures.||
12308|Moranbah Coal Measures|73625|6|Mentioned|p5 Fig.3, p13, 21, p23 Fig.14C|Permian|Permian|Nebo Synclinorium, Bowen Basin.||||Overlies German Creek Coal Measures. Is overlain by Fort Cooper Coal Measures.||
12308|Moranbah Coal Measures|75060|6|Mentioned|p43, 46, 50, 53, 55|Pemian|Permian|Bowen Basin.|||||A mixture of coal, laminated and carbonaceous siltstone, mudstone, sandstone and tuffs.|
12359|Mort Member|22954|4|Described|Fig1p6,17,22-3|Warendan|Datsonian|||||||
12359|Mort Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
12359|Mort Member|37572|4|Described|p162|||||||||
12359|Mort Member|38532|4|Described|p242|||||||||
12359|Mort Member|40136|5|Briefly described|p32|||||||||
12359|Mort Member|40852|6|Mentioned|Fig.3.7|||||||||
12359|Mort Member|46897|6|Mentioned|Fig.2|||||||||
12359|Mort Member|46958|6|Mentioned|p195|||||||||
12359|Mort Member|50244|6|Mentioned|p89 Fig. 1, p100 Fig. 7|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||22-APR-09
12359|Mort Member|64068|4|Described|p74|Early Ordovician|Late Cambrian|124 m thick in type section.||Of Ninmaroo Formation.||Overlies Jiggamore Member. Is overlain by Corrie Member.|Flat-pebble limestone conglomerate, intraformational breccia, peloid-ooid and peloid-intraclast grainstone; minor stromatolite boundstone, thrombolite boundstone.|10-APR-12
12359|Mort Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin.||Cockroach Group|||Limestone (intraclast, ooid and peloid grainstone), calcareous siltstone.|
12402|Moses Sandstone|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
12402|Moses Sandstone|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
12402|Moses Sandstone|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
12402|Moses Sandstone|34485|4|Described|Table 1|||Tertiary||||||
12402|Moses Sandstone|37607|6|Mentioned|p332|||See also Fig.4.||||||
12402|Moses Sandstone|39445|5|Briefly described|Table 14|||||||||
12402|Moses Sandstone|44017|14|Not recorded|Map Legend||Tertiary|||||||
12402|Moses Sandstone|44018|14|Not recorded|Map Legend||Tertiary|||||||
12402|Moses Sandstone|44087|14|Not recorded|p8,9,opp.7||Tertiary|||||||
12402|Moses Sandstone|44090|14|Not recorded|Map Legend||Tertiary|||||||
12402|Moses Sandstone|44222|14|Not recorded|p121|||Unconformable on Mackunda Beds and Winton Formation.||||||
12402|Moses Sandstone|44291|14|Not recorded|p9|||||||||
12402|Moses Sandstone|44351|14|Not recorded|p10||Tertiary|Overlain by Springvale Formation. (Early Tertiary)||||||
12402|Moses Sandstone|44413|2|Defined|p470,471||Tertiary|||||||
12402|Moses Sandstone|44836|14|Not recorded|p11,238||Tertiary|||||||
12402|Moses Sandstone|45145|6|Mentioned|Table 7|||||||||
12402|Moses Sandstone|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
12402|Moses Sandstone|61155|5|Briefly described|p16|Middle Eocene|Early Eocene|Age: <57Ma. Max. thickness: 80m. Geological region: Diamantina.||||||
12402|Moses Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Fluviatile silicified quartzose sandstone, laminar siltstone, mudstone; sandy ironstone at base.|
12402|Moses Sandstone|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Oakdale Sandstone, and unnamed units, are all mapped under the symbol, Tl.||||||
12402|Moses Sandstone|69599|5|Briefly described|p584, p599|Eocene|Paleocene|Vine (1964). ~19m thick. Springvale Basin. RELATED UNITS (continued): Correlated (at least partly) with Moonie, Eyre, Glendower, Edkins, Springvale and Marion Formations; Werite and Old Cork beds; and Mueller Sandstone.||||Unconformably overlies Mackunda and Winton Formations. Is overlain unconformably by Springvale Formation. See COMMENTS for more.|Fine-grained, partly silicified and ferruginised fluvial sandstone.|
12423|Mossman Granite|41740|6|Mentioned|p222|||||||||
12435|Mount Abbot Igneous Complex|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
12435|Mount Abbot Igneous Complex|31984|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12435|Mount Abbot Igneous Complex|32553|4|Described|p56|||||||||
12435|Mount Abbot Igneous Complex|32556|4|Described|Table 4|||L.Cret.||||||
12435|Mount Abbot Igneous Complex|34894|6|Mentioned|p483|||||||||
12435|Mount Abbot Igneous Complex|34975|6|Mentioned|p914|||||||||
12435|Mount Abbot Igneous Complex|36472|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
12435|Mount Abbot Igneous Complex|38365|6|Mentioned|p11|||||||||
12435|Mount Abbot Igneous Complex|39445|5|Briefly described|Table 12|||||||||
12435|Mount Abbot Igneous Complex|45151|5|Briefly described|Table 12|||||||||
12435|Mount Abbot Igneous Complex|48922|3|Fully described|p61|||Structural relationships P37.||||||
12435|Mount Abbot Igneous Complex|65706|4|Described|p12, Tb.1 p15,16,18; p47, p84,|Early Cretaceous|Early Cretaceous|Subvolcanic complex, probably associated with ring-fracturing. Felsite cone sheets. Hosts extensive zones of anomalous Cu at the Stockyard Creek Prospect.|||||Alkali granite, quartz syenite, quartz monzodiorite.|
12435|Mount Abbot Igneous Complex|68679|6|Mentioned|p366 Fig.5.56|Early Cretaceous|Early Cretaceous|Geochemical plots showing exceptionally high Na2O content.||||||
12435|Mount Abbot Igneous Complex|69594|5|Briefly described|p567, p569, p570 Fig.7.44, p571 Fig.7.47|Early Cretaceous|Early Cretaceous|Bowen-Mackay region. ~55km WSW of Bowen. Geochemical plots. The silicic rocks are the richest in alkalis of the Cretaceous intrusions in the Bowen region; the quartz syenite borders on peralkaline.|119.3 +/- 2.2 Ma (SHRIMP: Allen et al. 1998).||||Mainly quartz syenite and biotite monzogranite, with minor clinopyroxene-biotite-hornblende quartz monzodiorite and rhyolite-microgranite cone sheets and dykes.|
12435|Mount Abbot Igneous Complex|70673|6|Mentioned|p116|||||||Possibly intrudes "Nevada granodiorite".||
12435|Mount Abbot Igneous Complex|71592|5|Briefly described|Appendix A.||||119+/-2.2 Ma (SHRIMP U-Pb zircon).||||Granite.|
12435|Mount Abbot Igneous Complex|73029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||2 unnamed subdivisions described.||Pale pinkish grey, medium-coarse, quartz syenite; with minor aegirine, aenigmatite and vuggy pegmatitic patches; fine to medium biotite-hornblende quartz monzodiorite, with traces of clinopyroxene, titanite. Leucocratic biotite granite.|
12435|Mount Abbot Igneous Complex|73450|4|Described|p4, p41-44, p69|Aptian|Aptian|Forms a dissected plateau W-SW of Bowen; forms cone sheets/ring dykes, which consist mainly of flow-banded rhyolite with common phenocrysts. Subunit 1 includes syenite-quartz monzonite with scattered miarolitic cavities and sparse 'dioritic' enclaves both up to ca 3 cm in diameter, and subunit 2 includes biotite granite with common miarolitic cavities and very scarce enclaves. Subunit 1 is intruded by subunit 2. Inclusions (sometimes exceeding 1 m across) of partly to extensively recrystallised, intermediate-felsic volcanics are locally abundant in the marginal zone of the intrusion. Subunit 1 yielded a K-Ar hornblende age of 116 +/- 4 Ma (Paine et al., 1974), which is within error of the U-Pb SHRIMP zircon age of 119 +/- 2 Ma for Subunit 2 (Allen et al., 1998).|119 +/- 2 Ma U-Pb SHRIMP|||Intrudes Kurungle Volcanics.|Syenite-quartz monzonite (variable grainsize) and fine grained biotite granite with rhyolite-microgranite and some rocks of intermediate, potassic composition.|
12441|Mount Albert Group|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Includes: Roxmere Quartzite.||||||
12441|Mount Albert Group|22461|6|Mentioned|p468|||Spelt Mt in text.||||||
12441|Mount Albert Group|22483|5|Briefly described|p417|||Correlation has been made with the Roxmere Quartzite. Spelt Mt in text.||||||
12441|Mount Albert Group|22522|6|Mentioned|p330-331,Fig2p332||Statherian|Max Age: 1625 Ma. Either overlies the Mary Kathleen Group with tectonised unconformity (Derrick et al. 1977b) or may be allochthonous (Laing 1993).||||||
12441|Mount Albert Group|23192|6|Mentioned|Fig.2|||||||||
12441|Mount Albert Group|23518|5|Briefly described|p9 Fig. 3|Proterozoic|Proterozoic|Geological Province: Eastern Fold Belt.||||||
12441|Mount Albert Group|24255|5|Briefly described|p32 Fig.1|||Geological Province: Eastern Succession, Mount Isa Block.||||||
12441|Mount Albert Group|24256|6|Mentioned|p54|||Geological Province: Mount Isa Block.||||||
12441|Mount Albert Group|24259|6|Mentioned|p105|||Geological Province: Mount Isa Block.||||||
12441|Mount Albert Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
12441|Mount Albert Group|30531|6|Mentioned|p15|||Also mention P20 and P22.||||||
12441|Mount Albert Group|30532|2|Defined|p115|Precambrian|Precambrian|||||||
12441|Mount Albert Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12441|Mount Albert Group|33900|4|Described|p18|||Mention P4||||||
12441|Mount Albert Group|35074|6|Mentioned|Fig.2|||||||||
12441|Mount Albert Group|36052|6|Mentioned|Fig.2|||||||||
12441|Mount Albert Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12441|Mount Albert Group|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
12441|Mount Albert Group|37462|4|Described|Table4.VII|||||||||
12441|Mount Albert Group|37565|5|Briefly described|p3|||See also Fig.5||||||
12441|Mount Albert Group|37568|5|Briefly described|p84|||||||||
12441|Mount Albert Group|37868|6|Mentioned|p207|||||||||
12441|Mount Albert Group|38243|6|Mentioned|p354|||||||||
12441|Mount Albert Group|38276|6|Mentioned|Fig.1|||||||||
12441|Mount Albert Group|38278|6|Mentioned|p8|||||||||
12441|Mount Albert Group|38833|6|Mentioned|p161|||||||||
12441|Mount Albert Group|39445|6|Mentioned|p36|||See also P42, P43 & Table 2||||||
12441|Mount Albert Group|39492|6|Mentioned|p28|||||||||
12441|Mount Albert Group|39622|6|Mentioned|Fig.2|||||||||
12441|Mount Albert Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12441|Mount Albert Group|39899|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12441|Mount Albert Group|39937|6|Mentioned|Fig.1|||||||||
12441|Mount Albert Group|40648|3|Fully described|p10|||||||||
12441|Mount Albert Group|40840|6|Mentioned|Map legend|||||||||
12441|Mount Albert Group|40984|4|Described|p389|||||||||
12441|Mount Albert Group|41272|5|Briefly described|M 1of1 C07|||||||||
12441|Mount Albert Group|41464|6|Mentioned|Map legend|Proterozoic||||||||
12441|Mount Albert Group|41556|6|Mentioned|Map legend|Proterozoic||||||||
12441|Mount Albert Group|41568|4|Described|p12|||||||||
12441|Mount Albert Group|41614|6|Mentioned|p145|||||||||
12441|Mount Albert Group|41744|5|Briefly described|p406|||||||||
12441|Mount Albert Group|41791|6|Mentioned|p255|||||||||
12441|Mount Albert Group|41978|6|Mentioned|p490|||||||||
12441|Mount Albert Group|41979|6|Mentioned|Fig.2 P512|||||||||
12441|Mount Albert Group|42173|6|Mentioned|Fig.1 P172|||||||||
12441|Mount Albert Group|42565|5|Briefly described|Table 1 P5, P3|||||||||
12441|Mount Albert Group|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Includes Deighton Quartzite and White Blow Formation. Feldspathic sandstone and pelitic and calcareous sedimentary rocks.||||||09-FEB-09
12441|Mount Albert Group|43595|5|Briefly described|p440-1|||||||||
12441|Mount Albert Group|43614|6|Mentioned|Fig.1|||||||||
12441|Mount Albert Group|43616|6|Mentioned|p4|||||||||
12441|Mount Albert Group|44195|6|Mentioned|p356 Fig.9|||||||||
12441|Mount Albert Group|45136|4|Described|Table 1|||||||||
12441|Mount Albert Group|45166|4|Described|p32|||||||||
12441|Mount Albert Group|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
12441|Mount Albert Group|46960|6|Mentioned|p218|||See also P220.||||||
12441|Mount Albert Group|46962|4|Described|Table 1|||See also Fig.3.||||||
12441|Mount Albert Group|46995|6|Mentioned|p269|||||||||
12441|Mount Albert Group|46996|6|Mentioned|p273|||||||||
12441|Mount Albert Group|49041|5|Briefly described|Table 1|||See also Table 3||||||
12441|Mount Albert Group|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Kalkadoon - Leichhardt Block and Eastern Fold Belt.||||||03-JUN-09
12441|Mount Albert Group|61922|5|Briefly described|p17 Fig. 9|||In the Mary Kathleen Zone.||||||
12441|Mount Albert Group|61929|5|Briefly described|p128 Fig. 2|||||||||
12441|Mount Albert Group|62047|6|Mentioned|p90 Fig.1 |||||||||
12441|Mount Albert Group|63055|5|Briefly described|p12 Fig. 1|||Part of Cover Sequence 3.||||||
12441|Mount Albert Group|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||3500 m thick.|Between c.1700 and 1670 Ma.||||Dolomite, siltstone, shale.|
12441|Mount Albert Group|64248|5|Briefly described|p32, p33 Fig.1, p36, p38 Fig.5 |||See also p40 Fig.6, p43 Fig.11, p44.|||Includes Deighton and Knapdale Quartzites; White Blow Formation; Lady Clayre Dolomite.|Equivalent to Soldiers Cap Group (lateral facies variation).||11-DEC-17
12441|Mount Albert Group|64250|5|Briefly described|Figs.2-5,8; p7, p18-19|||Status of this unit is uncertain.|1675-1610||Includes Deighton Quartzite, White Blow Formation, Knapdale Quartzite and Lady Clayre Dolomite.|No direct age constraints. Contacts with underlying rocks are uncertain. Placed now in Cover Sequence 3; tentative possible lateral facies equivalents of Soldiers Cap Group rocks.||
12441|Mount Albert Group|64251|6|Mentioned|p51 Fig. 1|||Geological Province: Mount Isa Inlier.||||||05-MAY-09
12441|Mount Albert Group|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: between ~1680-1610Ma.||||||
12441|Mount Albert Group|65387|6|Mentioned|p1|||Age is uncertain.|||Includes Knapdale Quartzite, Coocerina Formation and Lady Clayre Dolostone.|||
12441|Mount Albert Group|65396|5|Briefly described|p4, p7, p15-16, p23, p43, p78, p82, p169|Calymmian|Statherian|See also p173-175, p179, p182-184, p188, p190, p199, p202, p213, p217, p221-222, p230, p234-241, p272. Kalkadoon-Leichhardt Belt, Mary Kathleen Fold Belt. Eastern succession, Cover Sequence 3. No geochronology, but probably deposited c.1675-1610 Ma. Appears as Mt Albert group on p230.|||Includes Deighton Quartzite, White Blow Formation, Knapdale Quartzite, Coocerina Formation, Lady Clayre Dolomite, Quamby Conglomerate.|Temporal equivalent of Soldiers Cap Group and Young Australia Group.||04-APR-17
12441|Mount Albert Group|65755|6|Mentioned|p3 Fig.1|||||||||
12441|Mount Albert Group|67323|4|Described|p15, p25-26, p33-34, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Widespread unit in the Mount Isa Inlier. Forms linear belts with generally low flat aeromagnetic response.|~1710 - 1670 Ma.||Coocerina Formation, Deighton Quartzite, Dugald River Shale Member, Knapdale Quartzite, Lady Clayre Formation, Mount Roseby Schist, White Blow Formation.|Unconformably overlies the Corella Formation.|Brown fine feldspathic and lithic sandstone, ferruginous mudstone, pebbly sandstone|
12441|Mount Albert Group|67539|5|Briefly described|p10|||Correlated with Landsborough Graben sandstones that are also similar to Ballara Quartzite.|||Includes Knapdale Quartzite and Deighton Quartzite.|Underlain by the Corella Formation ?||
12441|Mount Albert Group|68146|5|Briefly described|p3, p99, p199-200|||Mary Kathleen and Marino-Stavely Domains.|||Deighton Quartzite, Lady Clayre Dolostone.|||
12441|Mount Albert Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
12441|Mount Albert Group|69056|6|Mentioned|p2-3, p5, p12|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area. See references to Lower Mount Albert Group (p4, p6, p13, p18, p23, p28, p36) and Upper Mount Albert Group (p4, p6, p13, p18, p23, p28, p55).|||Deighton, Knapdale Quartzites; Mount Roseby Schist; Coocerina, White Blow, Lady Clayre Formations.|||
12441|Mount Albert Group|69222|6|Mentioned|p222 Fig.2|Statherian|Statherian|Eastern Fold Belt.||||Overlies Ballara Quartzite||
12441|Mount Albert Group|69591|5|Briefly described|p29, p39, p45, p56, p107|Paleoproterozoic|Paleoproterozoic|Originally defined by Derrick, Wilson and Hill (1977). Kalkadoon-Leichhardt and Mary Kathleen Domains, Calvert Superbasin.|~1710 Ma.||Coocerina, Lady Clayre, White Blow Formations; Mount Roseby Schist; Knapdale, Deighton and ? Roxmere Quartzites.||Siliciclastic sediments.|
12441|Mount Albert Group|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Staveley Formation, Roxmere Quartzite.|||
12441|Mount Albert Group|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Staveley Formation, Roxmere Quartzite.|||
12441|Mount Albert Group|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Staveley, Coocerina, Lady Clayre Formations; Roxmere Quartzite; Mount Roseby Schist.|||
12441|Mount Albert Group|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Staveley, Coocerina, Lady Clayre Formations; Roxmere Quartzite; Mount Roseby Schist.|||
12441|Mount Albert Group|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Knapdale Quartzite, Mount Roseby Schist, Coocerina and Lady Clayre Formations.||Sandstone, siltstone, shale, conglomerate, dolostone, marble, mica schist, quartzite.|
12441|Mount Albert Group|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Roxmere Quartzite, Staveley Formation.|Is overlain by Kuridala Group and Answer Slate.||05-MAY-16
12441|Mount Albert Group|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||Includes Staveley Formation, Roxmere Quartzite|||
12441|Mount Albert Group|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||Includes Staveley Formation.|||
12441|Mount Albert Group|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||Includes Staveley Formation.|||
12441|Mount Albert Group|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Where undivided, described as quartzite and brown, fine-grained feldspathic and lithic sandstone, ferruginous mudstone, pebbly sandstone, variably dolomitic sandstone and siltstone and minor dolostone.|||Includes Lady Clayre Formation, Coocerina Formation, Mount Roseby Schist, Knapdale Quartzite.|||22-JUN-16
12441|Mount Albert Group|72596|6|Mentioned|p4|||Distribution shown in Fig i.||||||
12441|Mount Albert Group|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Doherty-Fig Tree Gully Domain, Marimo-Staveley Domain and Kuridala-Selwyn Domain.|||Includes Staveley Formation, Roxmere Quartzite.|||
12441|Mount Albert Group|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Doherty-Fig Tree Gully Domain, Marimo-Staveley Domain and Kuridala-Selwyn Domain.|||Includes Staveley Formation, Roxmere Quartzite.|||
12441|Mount Albert Group|72799|6|Mentioned|p4|||||||||
12441|Mount Albert Group|72889|6|Mentioned|p6 Fig.i.|||||||||
12441|Mount Albert Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
12441|Mount Albert Group|73413|6|Mentioned|p3|||Mount Isa Inlier. Included in Cover Sequence 3 of Foster and Austin (2008).||||||
12441|Mount Albert Group|73418|6|Mentioned|p4, p12|||Mary Kathleen Domain. Appears as Mount Albert group p4.|||||Largely schistose metasedimentary rocks.|
12441|Mount Albert Group|73529|5|Briefly described|p2 Fig.1, p4-5|||Calvert Superbasin, Mary Kathleen Domain. Reflects a transition from shallow marine to deep marine settings.|||Deighton Quartzite, Knapdale Quartzite, Coocerina Formation, White blow Formation, Mount Roseby Schist, Lady Clayre Formation|Unconformably overlies Mary Kathleen Group||
12441|Mount Albert Group|73553|4|Described|p1, p7-8, p178 Tb.5.9.2, p186-187|Statherian|Statherian|Mary Kathleen Domain. Included in the Calvert Superbasin assemblage in recent interpretations.|~1728-1686 Ma maximum depositional ages||Knapdale Quartzite, Dugald River Shale Member, Roseby Schist, Coocerina Formation, Lady Clayre Formation, Deighton Quartzite, White Blow Formation||Shallow to deep-marine metasedimentary rocks.|
12447|Mount Alford Ring Complex|39445|5|Briefly described|Table 14|||||||||
12447|Mount Alford Ring Complex|40623|5|Briefly described|p36|||||||||
12447|Mount Alford Ring Complex|44091|14|Not recorded|p66||Tertiary|||||||
12447|Mount Alford Ring Complex|44781|2|Defined|p363|||||||||
12447|Mount Alford Ring Complex|44783|14|Not recorded|p26|||||||||
12447|Mount Alford Ring Complex|44784|14|Not recorded|p13||Tertiary|||||||
12447|Mount Alford Ring Complex|44813|14|Not recorded|p81,90||Tertiary|22-24 Ma.||||||
12447|Mount Alford Ring Complex|48917|4|Described|p36|||||||||
12476|Mount Baldwin Formation|9694|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Underlies Errarra Formation, Arthur Creek Formation; overlies Elkera Formation. Geological Province: Georgina Basin. Sandstone; rare siltstone.||||||07-NOV-06
12476|Mount Baldwin Formation|12891|5|Briefly described|p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: SW Georgina Basin. Written as Mt Baldwin Fm in text of figure.||||||07-FEB-11
12476|Mount Baldwin Formation|12951|5|Briefly described|p143, 145, 149, 155|Early Cambrian|Early Cambrian|Georgina Basin. Alluvial fan/ fan-delta setting.||||Laterally equivalent to Adam Shale. Unconformably overlies Elkera Formation.|Siliciclastic rocks.|
12476|Mount Baldwin Formation|22646|6|Mentioned|p 102|Early Cambrian||Situated in the Georgina Basin.  Mount is Mt in text.||||||07-NOV-06
12476|Mount Baldwin Formation|22954|6|Mentioned|Fig3p9|Early Cambrian||||||||
12476|Mount Baldwin Formation|24581|6|Mentioned|p817|Cambrian|Cambrian|Mount is Mt. in text. Geological Province: Georgina Basin.||||||
12476|Mount Baldwin Formation|33103|6|Mentioned|p23|||||||||
12476|Mount Baldwin Formation|33111|6|Mentioned|p38|||p39.||||||07-NOV-06
12476|Mount Baldwin Formation|33681|6|Mentioned|p137|||||||||
12476|Mount Baldwin Formation|35005|5|Briefly described|p145|||||||||
12476|Mount Baldwin Formation|35221|6|Mentioned|p14|||||||||
12476|Mount Baldwin Formation|35798|6|Mentioned|p307|||Early Cambrian. Correlative of Adam Shale and lower Red Heart Dolomite.||||||07-NOV-06
12476|Mount Baldwin Formation|37572|5|Briefly described|p154|||See also p156,165 and Fig.8.||||||07-NOV-06
12476|Mount Baldwin Formation|38157|6|Mentioned|Table IX|||||||||
12476|Mount Baldwin Formation|38445|6|Mentioned|p102|||||||||
12476|Mount Baldwin Formation|39210|4|Described|p51|||Age p53.||||||07-NOV-06
12476|Mount Baldwin Formation|40538|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Quartz arenite, medium to coarse grained, thin to thick bedded, dusky red. Geological Province: Georgina Basin.||||||15-NOV-05
12476|Mount Baldwin Formation|40642|6|Mentioned|p163|||||||||
12476|Mount Baldwin Formation|40810|5|Briefly described|p13|||||||||
12476|Mount Baldwin Formation|40906|4|Described|p21|||||||||
12476|Mount Baldwin Formation|41457|6|Mentioned|p24|||||||||
12476|Mount Baldwin Formation|41524|6|Mentioned|Fig.3|||||||||
12476|Mount Baldwin Formation|41801|6|Mentioned|p214|||||||||
12476|Mount Baldwin Formation|42059|6|Mentioned|Fig.2 P131|||||||||
12476|Mount Baldwin Formation|42504|5|Briefly described|p85|||||||||
12476|Mount Baldwin Formation|42643|6|Mentioned|p21|||In the HUCKITTA sheet area.||||||07-NOV-06
12476|Mount Baldwin Formation|42956|4|Described|p30|||see also Fig.4 p31.||||||07-NOV-06
12476|Mount Baldwin Formation|44320|14|Not recorded|p.7|||||||||
12476|Mount Baldwin Formation|44327|2|Defined|Tb.I,p.8-10,18,map||Middle Cambrian|(F53-11). Mid Camb.top fm. Of the Mopunga Group.||||||07-NOV-06
12476|Mount Baldwin Formation|44328|14|Not recorded|map legend|Early Cambrian|Neoproterozoic|Lower Cambrian to Upper Proterozoic.||||||
12476|Mount Baldwin Formation|44358|5|Briefly described|p8||Early Cambrian|In HUCKITTA sheet area.||||||07-NOV-06
12476|Mount Baldwin Formation|45052|2|Defined|p68|Adelaidean|Adelaidean|||||||
12476|Mount Baldwin Formation|45102|6|Mentioned|p4|||See also p45.||||||07-NOV-06
12476|Mount Baldwin Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||07-NOV-06
12476|Mount Baldwin Formation|45155|6|Mentioned|Fig.8|||||||||
12476|Mount Baldwin Formation|46957|4|Described|p166|||||||||
12476|Mount Baldwin Formation|47035|6|Mentioned|p85|||||||||
12476|Mount Baldwin Formation|48844|2|Defined|p.26-37||Early Cambrian|On many pages. p.1,16-7,20,26-37,39,41,43, F.26,58-9,65,67, Pl.8.(new name).Overlies Grant Bluff Formation. L.Cam.(F53-11). See also Fig.10, p26.||||||19-MAY-17
12476|Mount Baldwin Formation|48901|14|Not recorded|Not recorded||Early Cambrian|L.Cambrian.||||||
12476|Mount Baldwin Formation|48990|1|Redefined|p13|Adelaidean|Adelaidean|See also p11.||||||07-NOV-06
12476|Mount Baldwin Formation|49027|6|Mentioned|p7|||||||||
12476|Mount Baldwin Formation|60122|6|Mentioned|p9 P11 Tb. 1|||Within Supersequence 4. Disconformably overlain by Red Heart Dolostone. Geological Province: Georgina Basin. See also p44.||||||
12476|Mount Baldwin Formation|60551|5|Briefly described|Map Legend|Cambrian|Cambrian|Underlies Errarra Formation, Arthur Creek Formation; overlies Elkera Formation. Geological province: Georgina Basin. Thin to thick bedded, cross bedded sandstone, rare siltstone.||||||30-SEP-08
12476|Mount Baldwin Formation|61022|5|Briefly described|p15 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E. Mount is MT in text.||||||20-APR-05
12476|Mount Baldwin Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group. Quartz arenite: medium to coarse.  Geological Province: southern Georgina Basin.||||||
12476|Mount Baldwin Formation|61732|6|Mentioned|p109, p113|||Overlies Elkera Formation. Formerly included a stromatolite section now in the upper part of the Elkera Formation.||||||07-FEB-11
12476|Mount Baldwin Formation|62376|5|Briefly described|p53|Early Cambrian|Neoproterozoic|Geological Province: Georgina Basin||||||09-FEB-10
12476|Mount Baldwin Formation|62595|6|Mentioned|p28 Fig.4.|Early Cambrian|Early Cambrian|Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
12476|Mount Baldwin Formation|62789|5|Briefly described|p128, p129 Fig. 2|Early Cambrian|Neoproterozoic|In southern Georgina Basin. 63 m thick at Pacific Oil & Gas Baldwin No. 1 exploration well.||||Underlies Lower Cambrian Red Heart Dolostone and overlies Mopunga Group.|Thickly bedded sandstone, lesser siltstone.|28-MAR-12
12476|Mount Baldwin Formation|62790|5|Briefly described|p208, 210|Early Cambrian|Neoproterozoic|Southern Georgina Basin. 63 m thick in Pacific Oil & Gas Baldwin No. 1 well.||||Overlies Mopunga Group and underlies Errarra Formation.|Thickly bedded sandstone, lesser siltstone.|28-MAR-12
12476|Mount Baldwin Formation|62984|5|Briefly described|p14|||Appears to conformably overlie the Elkera Formation. Geological Province: Georgina Basin.||||||23-JAN-07
12476|Mount Baldwin Formation|63562|4|Described|p338 fig 3, p345-8, p351, p352 fig 10|Early Cambrian|Early Cambrian|Of Georgina Basin. Zircons have several age clusters; possible source areas discussed.||||Correlated with Arumbera Sandstone.|Well-sorted, medium- to fine-grained quartz sandstone; contains earliest Cambrian trace fossils.|
12476|Mount Baldwin Formation|64068|3|Fully described|p55, p51, 54, p19, p ix|Early Cambrian|Early Cambrian|Potential hydrocarbon reservoir. Redefined (Walter 1980), to exclude upper dolostone now part of Red Heart Dolostone. Also removed from Mopunga Group in 1980. Correlations: Octy Formation, Neutral Junction Formation, Adam Shale, possibly Sylvester Sandstone.||Of Shadow Group.||Unconformably overlies Elkera Formation. Is unconformably overlain by Red Heart Dolostone.|Red to red-brown quartz arenite and sublitharenite, quartz greywacke, siltstone, shale; minor subarkose.|04-APR-12
12476|Mount Baldwin Formation|64778|6|Mentioned|p13|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin.||||||
12476|Mount Baldwin Formation|64812|5|Briefly described|p237 Fig. 2|Early Cambrian|Early Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
12476|Mount Baldwin Formation|64813|5|Briefly described|p256 Fig. 3|Early Cambrian|Early Cambrian|Unconformably overlies Elkera Formation; overlain by Red Heart Dolostone. Geological Province: southern Georgina Basin. Siliciclastic rocks.||||||11-FEB-09
12476|Mount Baldwin Formation|65237|5|Briefly described|p3 Fig. 4, p5|Early Cambrian|Early Cambrian|Unconformably on Elkera Fm in the south. Max.thickness: ~300m. Geol.prov: southern Georgina Basin. Full spectrum of alluvial fan-delta facies varying from proximal conglomeratic facies to distal siltstone/mudstone successions. Mount is Mt in places.||||||07-FEB-11
12476|Mount Baldwin Formation|65341|5|Briefly described|p14, p16. |||Previously (Smith 1964) included in Mopunga Group; later removed (Walter 1980) because of a local basal unconformity and Cambrian trace fossils. More recent field comparisons suggest that some outcrops mapped as Mount Baldwin Formation are likely laterally equivalent to parts of Central Mount Stuart Formation and Octy Formation and thus should be included in Mopunga Group.||||Overlies Elkera Formation.||
12476|Mount Baldwin Formation|66767|5|Briefly described|p59|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.|Fan-delta to marine sandstones.|
12476|Mount Baldwin Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Is overlain by Red Heart Dolostone.||12-JUL-16
12476|Mount Baldwin Formation|69443|4|Described|p28:7, 11, 14-15, 45-46|Early Cambrian|Early Cambrian|K.G. Smith (1964), redefined by Walter (1980). Southern Georgina Basin. 60-320m thick. Basal beds are recessive; the rest of the Formation is ridge-forming. Has been modelled for unconformity-related uranium mineralisation.||Shadow Group.||Disconformably or unconformably overlies Elkera Formation. Is overlain unconformably by Red Heart Dolostone. Correlated with Octy and Neutral Junction Formations, Adam Shale and ?Sylvester Sandstone.|Quartz sandstone, sublithic sandstone, quartz greywacke, siltstone, shale and minor subarkose. Rare granule-bearing beds and pebble-sized claystone intraclasts; prominent cross-beds throughout; various ichnofossils.|12-JUL-16
12476|Mount Baldwin Formation|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Red Heart Dolostone||
12476|Mount Baldwin Formation|69673|5|Briefly described|p116, p119 fig 94, p129, p136, p138|||||Shadow Group||Unconformably overlies Elkera Formation, unconformably overlain by Red Heart Dolostone, correlated with Octy Formation, Neutral Junction Formation|Quartz sandstone, sublithic sandstone, glauconitic and feldspathic sandstones, quartz greywacke, siltstone, shale and minor subarkose.|
12476|Mount Baldwin Formation|69917|6|Mentioned|p115|||Georgina Basin. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin.||||||
12476|Mount Baldwin Formation|70094|6|Mentioned|p80|||Detrital zircons from this and other units were analysed to establish similar provenances for Harts Range Group, Amadeus and Georgina Basins.||||||
12476|Mount Baldwin Formation|70749|6|Mentioned|p52-53|||Georgina Basin. Detrital zircons indicate a range of ages and more complex source(s).||||||
12476|Mount Baldwin Formation|70839|5|Briefly described|p344|||Of Georgina Basin. Part of Supersequence 4 equivalent to Amadeus Basin. Includes some late Mesoproterozoic age components that could be derived from the Musgrave region (c. 1.17 Ga; Maidment et al., 2007).||||||
12476|Mount Baldwin Formation|70951|6|Mentioned|p1077, 1082|||||||||
12476|Mount Baldwin Formation|71800|5|Briefly described|p26-p27|Early Cambrian|Early Cambrian|Georgina Basin.|||||Quartz sandstone.|
12476|Mount Baldwin Formation|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains Ichnofossils.||Shadow Group||Unconformably overlain by the Red Heart Dolostone.|Quartz arenite, sublitharenite; medium-thick-bedded, cross bedded; minor quartzwacke, siltstone, shale, granule-bearing greywacke, sandstone and coarse grained subarkose.|
12476|Mount Baldwin Formation|72516|3|Fully described|p12-13, p15, p61, p89-90, p95-96|Terreneuvian|Terreneuvian|Georgina Basin. Type section is defined in the Elua Range in JINKA. Exposed northeast of the Lucy Creek Fault Zone, Elua Range in the Jervois and Johansen Ranges and is structurally emplaced in the Charlotte Fault Zone. The basal beds are recessive whereas the rest of it is ridge-forming. Contains ichnofossils. 100-320m thick in Jervois Range, 230m thick in Johannsen Range. Deposited in an alluvial fan delta. Interpreted to correlate with the Octy Formation, Junction Formation, Adam Shale and Sylvester Sandstone. Age correlative of Crossing Bore Schist, Atula calc-silicate, Arumbera Sandstone. Intruded by quartz-vein breccias in the Charlotte and Bonya fault zones. See also p99, p154-155, p173, p176, p186.|ca 670 Ma (max dep age)|Shadow Group||Overlies the Elkera Formation with angular unconformity and the Thring Granite. Unconformably overlain by the Red Heart Dolostone.|Quartz arenite, sublitharenite; medium-thick bedded, cross bedded. Minor quartzwacke, siltstone, shale, granule-bearing greywacke, sandstones with pebble-sized claystone intraclasts, coarse grained subarkose.|02-JUN-21
12480|Mount Barker Granodiorite|23042|5|Briefly described|Fig 2||Cretaceous|||||||
12480|Mount Barker Granodiorite|23052|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
12480|Mount Barker Granodiorite|23161|4|Described|p47 table6|Early Cretaceous|Early Cretaceous|Ages: 122Ma to 125Ma.||||||
12480|Mount Barker Granodiorite|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
12480|Mount Barker Granodiorite|32553|4|Described|p56|||||||||
12480|Mount Barker Granodiorite|34314|6|Mentioned|p12|||||||||
12480|Mount Barker Granodiorite|39445|5|Briefly described|Table 12|||||||||
12480|Mount Barker Granodiorite|41246|6|Mentioned|Map legend|Cretaceous||||||||
12480|Mount Barker Granodiorite|42701|4|Described|p100|Early Cretaceous||||||||
12480|Mount Barker Granodiorite|43988|14|Not recorded|Map Legend||Early Cretaceous|||||||
12480|Mount Barker Granodiorite|43994|14|Not recorded|Map Legend|||||||||
12480|Mount Barker Granodiorite|43998|4|Described|p22|||||||||
12480|Mount Barker Granodiorite|44001|14|Not recorded|Map Legend||Mesozoic|||||||
12480|Mount Barker Granodiorite|44245|5|Briefly described|Map Legend||Cretaceous|||||||
12480|Mount Barker Granodiorite|44337|5|Briefly described|Map Legend||Cretaceous|Lithology.||||||
12480|Mount Barker Granodiorite|45071|3|Fully described|Table 15|||||||||
12480|Mount Barker Granodiorite|45087|5|Briefly described|p48|||Chemical analyses.||||||
12480|Mount Barker Granodiorite|48841|14|Not recorded|p19,43,46,49|||||||||
12480|Mount Barker Granodiorite|48894|6|Mentioned|p39|||Age.||||||
12480|Mount Barker Granodiorite|65388|5|Briefly described|p406|||Intrudes Bowen Basin, along with Gotthardt Granodiorite, and Bundarra Granodiorite further east. All have also produced metamorphic aureole in surrounding sediments too.||||||
12480|Mount Barker Granodiorite|69594|5|Briefly described|p571 Figs.7.45-46|Early Cretaceous|Early Cretaceous|Southern Connors Subprovince, Bowen Basin. Geochemistry plots.||||||
12480|Mount Barker Granodiorite|73037|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||||Hornblende, biotite granodiorite, diorite.|
12484|Mount Barney Central Complex|31694|6|Mentioned|p347|||||||||
12484|Mount Barney Central Complex|32924|6|Mentioned|p111|||Refers Stephenson (1956, 1959)||||||
12484|Mount Barney Central Complex|39445|5|Briefly described|Table 14|||||||||
12484|Mount Barney Central Complex|40780|4|Described|p11|||||||||
12484|Mount Barney Central Complex|40896|4|Described|p51|||||||||
12484|Mount Barney Central Complex|44091|14|Not recorded|p66||Tertiary|||||||
12484|Mount Barney Central Complex|44778|2|Defined|p135|||(Post Triassic - pre Eocene-Oligocene)||||||
12484|Mount Barney Central Complex|44781|2|Defined|p362|||Emplaced in Middle Carboniferous sediments.||||||
12484|Mount Barney Central Complex|44784|14|Not recorded|p12||Tertiary|||||||
12484|Mount Barney Central Complex|44813|14|Not recorded|p81||Tertiary|Intruded into Middle Carboniferous 23.4 Ma.||||||
12484|Mount Barney Central Complex|45014|14|Not recorded|p20|||SE Qld||||||
12484|Mount Barney Central Complex|48917|5|Briefly described|p36|||Refers Stephenson (1959,1960)||||||
12484|Mount Barney Central Complex|48928|6|Mentioned|p15|||||||||
12484|Mount Barney Central Complex|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as the Silver Plains Nephelinite, Tabor Gabbro, Mount Jukes Intrusive Complex, and unnamed basaltic to rhyolitic plugs, are all mapped under the symbol, Ti.||||||
12484|Mount Barney Central Complex|73450|4|Described|p96-98|||Comprises the core and defining feature of the Focal Peak volcano. Associated intrusive structures include ring dykes, cone sheets, a broad dome and a closed ring fault.|||||A suite of dominantly felsic, high-level, intrusive and less common extrusive igneous rocks including diorites, dolerites, microsyenites, granophyres, rhyolites and trachytes as well as mafic to felsic pyroclastic rocks.|
12490|Mount Barney beds|23799|6|Mentioned|p126 Fig. 24|||Geological Province: Yarrol Province.||||||
12490|Mount Barney beds|30772|6|Mentioned|p1|||Fauna||||||
12490|Mount Barney beds|40623|5|Briefly described|p40|||||||||
12490|Mount Barney beds|40780|4|Described|p4|||||||||
12490|Mount Barney beds|40896|6|Mentioned|p47|||||||||
12490|Mount Barney beds|43008|5|Briefly described|map legend|||||||||
12490|Mount Barney beds|44372|6|Mentioned|p41|||||||||
12490|Mount Barney beds|61007|6|Mentioned|p293|Carboniferous|Carboniferous|||||||
12490|Mount Barney beds|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit is mapped with Alice Creek beds under the symbol, Cy.||||||
12490|Mount Barney beds|68679|5|Briefly described|p306, p321, p350-351|Pennsylvanian|Pennsylvanian|Stephenson (1959); Olgers et al. (1974). Occurs in two down-faulted belts E and W of Mount Barney near the NSW border. Yarrol Province forearc rocks. Similar clasts noticed in rocks in Beenleigh Subprovince and in NSW: significance for possible extent of the Subprovince mentioned.||||Is intruded by Mount Barney Igneous Complex.|Basal calc-silicate rocks, overlain by lithic and feldspathic sandstone with interbedded rhyolitic and trachytic lava flows and tuffs, and dark fine-grained siltstone with spiriferoid brachiopods; then sandstone, conglomerate and crinoidal mudstone.|
12490|Mount Barney beds|69599|6|Mentioned|p640|Paleozoic|Paleozoic|Exposed around the Focal Peak volcano at Mount Barney.||||||
12504|Mount Bauple Syenite|24382|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
12504|Mount Bauple Syenite|30655|6|Mentioned|p38|||||||||
12504|Mount Bauple Syenite|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
12504|Mount Bauple Syenite|34949|6|Mentioned|p155|||||||||
12504|Mount Bauple Syenite|36926|6|Mentioned|p168|||||||||
12504|Mount Bauple Syenite|37118|6|Mentioned|p318|||||||||
12504|Mount Bauple Syenite|39445|5|Briefly described|Table 12|||||||||
12504|Mount Bauple Syenite|42894|5|Briefly described|p29|||||||||
12504|Mount Bauple Syenite|44752|14|Not recorded|p299|||Intrudes Tiaro Coal Measures.||||||
12504|Mount Bauple Syenite|45440|4|Described|p.61,62,63,87|Cretaceous|Jurassic|Tb.1.||||||
12504|Mount Bauple Syenite|63821|4|Described|p33|Early Cretaceous|Late Jurassic|Age: 138+/-4Ma (K-Ar biotite). Intrudes Tiaro C.M. (forming zones of graphite) and Grahams Creek Formation. Comprises biotite-quartz syenite.||||||07-FEB-11
12504|Mount Bauple Syenite|68553|6|Mentioned|Map legend|Cretaceous|Jurassic|This unit, as well as the Noosa Quartz Diorite, Mount Urah Granodiorite, and unnamed intrusive units, are all mapped under the symbol, JKi.||||||
12504|Mount Bauple Syenite|68679|6|Mentioned|p312|Cretaceous|Jurassic|Northern New England Orogen.||||||
12504|Mount Bauple Syenite|69594|5|Briefly described|p560-562|Early Cretaceous|Early Cretaceous|Ellis (1968); Cranfield (1994). Whitsunday Volcanic Province. Western side of Mount Bauple. Probably more extensive at depth.|138 +/- 4 Ma (Green and Webb, 1974).|||Intrudes Tiaro Coal Measures.|Medium- to coarse-grained biotite-quartz syenite with anhedral perthitic K-feldspar, oligoclase, fractured quartz, subhedral biotite, and rare hornblende and magnetite.|
12516|Mount Birnie beds|32576|6|Mentioned|Fig.2|||||||||
12516|Mount Birnie beds|37816|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
12516|Mount Birnie beds|37930|6|Mentioned|p528|||||||||
12516|Mount Birnie beds|38350|6|Mentioned|p22|||||||||
12516|Mount Birnie beds|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12516|Mount Birnie beds|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
12516|Mount Birnie beds|39425|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
12516|Mount Birnie beds|39496|6|Mentioned|p16|||||||||
12516|Mount Birnie beds|41306|6|Mentioned|p6|||||||||
12516|Mount Birnie beds|41801|6|Mentioned|p217|||||||||
12516|Mount Birnie beds|45162|6|Mentioned|p153|||||||||
12516|Mount Birnie beds|49027|6|Mentioned|p7|||||||||
12516|Mount Birnie beds|50100|5|Briefly described|p22|Early Cambrian|Early Cambrian|Predominantly shallow-marine, clastic, calcareous, dolomitic, cherty and phosphatic sedimentary rocks.  Disconformably overlain by Thorntonia Limestone.||||||
12516|Mount Birnie beds|63450|5|Briefly described|p78 Fig. 5, p80|Early Cambrian|Early Cambrian|Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
12516|Mount Birnie beds|64068|4|Described|p54, p46, 58|Early Cambrian|Early Cambrian|Correlations: Mount Baldwin Formation, Adam Shale, Octy Formation, Neutral Junction Formation, Riversdale Formation and possibly Sylvester Sandstone.||Of Shadow Group.||Unconformably overlies Little Burke Tillite. Is overlain unconformably by Thorntonia Limestone or Beetle Creek Formation.|Conglomerate, orthoquartzitic, silty and ferruginous sandstones, arkose, red and green micaceous shale, siltstone.|05-APR-12
12516|Mount Birnie beds|67127|6|Mentioned|p80|||||||||
12516|Mount Birnie beds|67323|5|Briefly described|GIS attrib tbl; p83|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Shadow Group||Is overlain unconformably by Thorntonia Limestone.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone, dolomite.|
12516|Mount Birnie beds|67870|5|Briefly described|p38-39, p43-46, p48, p50-53|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin. Basal sequence in the Basin.||||Is overlain unconformably by Thorntonia Limestone.|Sandstone, dolostone, organic-rich siltstone, shale.|
12516|Mount Birnie beds|68270|5|Briefly described|p681,683|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Underlain unconformably by Little Burke Tillite.||
12516|Mount Birnie beds|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Shadow Group|||Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite|
12516|Mount Birnie beds|69443|5|Briefly described|p28:7, 14|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||||12-JUL-16
12516|Mount Birnie beds|69591|5|Briefly described|p87, p90-93, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Shadow Group.||Is overlain unconformably by Thorntonia Limestone. A notional correlative of Riversdale Formation.|Basal tillite(20m); bedded dolomite(10m); massive dark ferruginous sandstone, thick-bedded and thin-bedded sandstone(40m); sandy, red or green micaceous shale and siltstone(100m); orthoquartzite and quartz conglomerate(20m); massive mudstone(20m).|
12516|Mount Birnie beds|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Shadow Group||Underlies Thorntonia Limestone.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
12516|Mount Birnie beds|72684|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Shadow Group||Shown as unconformably underlying the Narpa Group.|Massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
12516|Mount Birnie beds|73553|5|Briefly described|p263|Cambrian|Neoproterozoic|Georgina Basin.||||Unconformably overlies Wimberu Granite||
12562|Mount Byron Volcanics|22845|6|Mentioned|p11  Fig6||Triassic|||||||
12562|Mount Byron Volcanics|22846|6|Mentioned|p44||Triassic|||||||
12562|Mount Byron Volcanics|24418|5|Briefly described|p5, Map 1|Late Triassic|Late Triassic|Consists of rhyolitic and trachytic volcanics. Main rock types are welded tuff, agglomerate, and lithic tuff, minor rhyolite, andesite, and basalt. Age: ~220Ma. Bounded by North Pine Fault.||||||30-JUN-06
12562|Mount Byron Volcanics|29720|6|Mentioned|Fig.1|||||||||
12562|Mount Byron Volcanics|30303|2|Defined|p323|Tertiary|Tertiary|Tweedale(1960). Prob. Tertiary||||||09-NOV-15
12562|Mount Byron Volcanics|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
12562|Mount Byron Volcanics|31811|6|Mentioned|Fig. 1|||||||||
12562|Mount Byron Volcanics|33881|6|Mentioned|p96|||||||||
12562|Mount Byron Volcanics|35007|6|Mentioned|p75|||||||||
12562|Mount Byron Volcanics|35101|3|Fully described|p46|||||||||
12562|Mount Byron Volcanics|35430|6|Mentioned|Fig.1|||Geological map.||||||
12562|Mount Byron Volcanics|36440|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
12562|Mount Byron Volcanics|36954|6|Mentioned|p115|||||||||
12562|Mount Byron Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
12562|Mount Byron Volcanics|38391|6|Mentioned|p10|||||||||
12562|Mount Byron Volcanics|38805|6|Mentioned|p83|||See also Fig.1||||||
12562|Mount Byron Volcanics|39079|5|Briefly described|p9|||||||||
12562|Mount Byron Volcanics|39445|5|Briefly described|Table 9|||See also Fig.7||||||
12562|Mount Byron Volcanics|40051|4|Described|p8|||||||||
12562|Mount Byron Volcanics|40245|6|Mentioned|p185|||Mention Fig.2||||||
12562|Mount Byron Volcanics|40479|6|Mentioned|p32|||||||||
12562|Mount Byron Volcanics|41738|6|Mentioned|p168|||||||||
12562|Mount Byron Volcanics|42525|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
12562|Mount Byron Volcanics|43008|5|Briefly described|map legend|||||||||
12562|Mount Byron Volcanics|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
12562|Mount Byron Volcanics|44925|5|Briefly described|Map Legend||Late Triassic|||||||
12562|Mount Byron Volcanics|60077|5|Briefly described|Map legend|Late Triassic|Late Triassic|Rhyolite, trachyte, basalt.||||||
12562|Mount Byron Volcanics|61772|6|Mentioned|p129||Late Triassic|Mountis Mt in text. In New England Orogen.||||||24-SEP-08
12562|Mount Byron Volcanics|65452|6|Mentioned|p4 Fig.1, p36|Late Triassic|Late Triassic|Southern Yarrol Province.||||||
12562|Mount Byron Volcanics|66855|6|Mentioned|p955.|||Written as Mt Byron in the article.||||||
12562|Mount Byron Volcanics|67203|6|Mentioned|p3|Triassic|Triassic|||||||
12562|Mount Byron Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Eagle, Ooramera, Portal Creek and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
12562|Mount Byron Volcanics|68679|5|Briefly described|p326, p386, p427, p434-435|Late Triassic|Late Triassic|Esk area. ~300m thick. May be comagmatic with Mount Mee Granophyre.|228.2 +/- 2.8 Ma (K-Ar: Murphy et al., 1987).|||Unconformably overlies Rocksberg Greenstone. Is faulted against and unconformably overlies Northbrook beds. Is intruded by Mount Mee Granophyre.|Basal andesitic lava flows with basaltic lavas and dacitic pyroclastics, overlain by more felsic rhyolitic pyroclastics and thick, spherulitic coherent rhyolite.|
12572|Mount Castle trachyte|39969|6|Mentioned|p10|||||||||
12572|Mount Castle trachyte|40542|6|Mentioned|p98|||||||||
12590|Mount Coley Sinter|37607|4|Described|p333|||See also Fig.4.||||||
12590|Mount Coley Sinter|39445|5|Briefly described|Table 14|||||||||
12590|Mount Coley Sinter|44308|14|Not recorded|Tb.2||Tertiary|||||||
12590|Mount Coley Sinter|44312|14|Not recorded|Map Legend||Tertiary|||||||
12590|Mount Coley Sinter|44351|14|Not recorded|p16,22,Fig.13|||Overlies Wilgunya Formation. Post-lateritic Tertiary age.||||||
12590|Mount Coley Sinter|44543|2|Defined|p35,36|||Probably similar age to Austral Downs Limestone. (Probably late Tertiary or younger)||||||
12590|Mount Coley Sinter|45052|5|Briefly described|p136|||Cainozoic||||||
12590|Mount Coley Sinter|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlies the Poodyea Formation. Age: ~16Ma. Thickness: 50m. Geological Province: Georgina Basin.||||||
12590|Mount Coley Sinter|63450|6|Mentioned|p83|Cenozoic|Cenozoic|Geological province: Georgina Basin.||||||07-FEB-11
12590|Mount Coley Sinter|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Brown and white cellular opaline sinter, milky blue and white massive chalcedony; spring deposits.|
12590|Mount Coley Sinter|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Austral Downs, Horse Creek and Noranside Limestones; Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
12590|Mount Coley Sinter|69599|5|Briefly described|p580, p584, p601|Miocene|Miocene|Reynolds (1966). Forms a series of isolated deposits in the MOUNT WHELAN 250k sheet area. Up to 50m thick. Widespread but individually localised, indicating several spring centres. Has Pliocene silcrete.||||Correlated with Doonbara, Whitula and Poodyea Formations; Noranside, Horse Creek and Austral Downs Limestones.|Chalcedonic and opaline silica.|
12591|Mount Coolon Andesite|23052|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
12591|Mount Coolon Andesite|23161|4|Described|p12|Early Carboniferous|Early Carboniferous|Age: 347+/-2.9 Ma.||||||
12591|Mount Coolon Andesite|23430|5|Briefly described|p510|||SHRIMP 347.0 +/- 2.9 Ma. Drummond Basin Province.||||||
12591|Mount Coolon Andesite|42701|3|Fully described|p32|||Reserved as Coolon Volcanics.||||||
12591|Mount Coolon Andesite|44245|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
12591|Mount Coolon Andesite|60659|5|Briefly described|p13, p61|Early Carboniferous|Early Carboniferous|Welded + unwelded andesitic to dacitic tuff. Intruded by Manaman Granodiorite. Hosts the Mount Coolon epithermal gold-silver deposit. Overlain by Locharwood Rhyolite (Bulgonunna Volcanics). Max. thickness: >300m. Age: 347.0+/-2.9Ma.||||||22-JUL-13
12591|Mount Coolon Andesite|68705|6|Mentioned|p41|||Koala Pit.  Age and estimates of mineralisation dates may be significantly younger than those of the Bimurra Volcanics.||||||
12591|Mount Coolon Andesite|68731|5|Briefly described|p193|Mississippian|Mississippian|Drummond Basin. Crops out over a small area near Mount Coolon. U-Pb zircon geochronology by Perkins, Walshe, and Morrison (1995).|347 +/- 3 Ma|||Overlain by the Bulgonunna Volcanic Group.|Comprises intermediate volcanics and volcaniclastics.|
12591|Mount Coolon Andesite|70740|5|Briefly described|i, p7, p8, p79-p80, p127|||Drummond Basin. Originally considered part of the Bulgonunna Volcanics but later grouped with Cycle one of the Drummond Basin. Age derived from Perkins et al, 1995. Hosts mineralisation in the Koala Mine.|347 +/- 2.9 Ma (SHRIMP U-PB)|||Intruded by the Manaman Granodiorite.|Heavily altered, poprhyritic, coherent dacite and welded to unwelded, andesitic to dacitic ignimbrite.|
12591|Mount Coolon Andesite|73035|5|Briefly described|Map legend|Carboniferous|Carboniferous||||||Welded and unwelded andesitic and dacitic tuff.|
12604|Mount Crosby Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Kholo Subgroup||||
12604|Mount Crosby Formation|24082|6|Mentioned|p453|||||||||
12604|Mount Crosby Formation|29386|6|Mentioned|p454|||Upper Triassic.||||||
12604|Mount Crosby Formation|30302|6|Mentioned|p414|||Refers Allen(1959)||||||
12604|Mount Crosby Formation|30458|6|Mentioned|p8|||Triassic age||||||
12604|Mount Crosby Formation|30465|6|Mentioned|p3|||||||||
12604|Mount Crosby Formation|30475|6|Mentioned|p164|||||||||
12604|Mount Crosby Formation|32136|6|Mentioned|p16|||Miospores. See also P27||||||
12604|Mount Crosby Formation|32180|5|Briefly described|p4|||||||||
12604|Mount Crosby Formation|33381|4|Described|p113|||Triassic. Kholo Sub-group. See also PP114,117||||||
12604|Mount Crosby Formation|33769|5|Briefly described|p149|||U.Triassic||||||
12604|Mount Crosby Formation|35161|6|Mentioned|p591|||||||||
12604|Mount Crosby Formation|35812|6|Mentioned|p570|||||||||
12604|Mount Crosby Formation|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
12604|Mount Crosby Formation|36440|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
12604|Mount Crosby Formation|36779|6|Mentioned|p6|||||||||
12604|Mount Crosby Formation|37111|5|Briefly described|p292|||||||||
12604|Mount Crosby Formation|38074|5|Briefly described|Table 1|||||||||
12604|Mount Crosby Formation|38076|6|Mentioned|Table 3|||||||||
12604|Mount Crosby Formation|38307|4|Described|p519|||||||||
12604|Mount Crosby Formation|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
12604|Mount Crosby Formation|39079|6|Mentioned|p10|||||||||
12604|Mount Crosby Formation|39445|5|Briefly described|Table 9|||||||||
12604|Mount Crosby Formation|40434|6|Mentioned|p25|||||||||
12604|Mount Crosby Formation|40623|5|Briefly described|p34|||||||||
12604|Mount Crosby Formation|41906|3|Fully described|Table 2 P18|||||||||
12604|Mount Crosby Formation|42336|5|Briefly described|Table 1 P5|||||||||
12604|Mount Crosby Formation|42539|5|Briefly described|p183|||||||||
12604|Mount Crosby Formation|43076|6|Mentioned|p19|||||||||
12604|Mount Crosby Formation|43922|14|Not recorded|p324-326|||"The microfloral evidence... suggests a Middle or Early Upper Triassic age." Formation of Kholo Subgroup of Ipswich Coal Measures.||||||
12604|Mount Crosby Formation|43923|6|Mentioned|p11|||||||||
12604|Mount Crosby Formation|43997|14|Not recorded|p113|||||||||
12604|Mount Crosby Formation|44026|14|Not recorded|p122||Triassic|Lithological equivalent of Neara Volcanics.||||||
12604|Mount Crosby Formation|44384|14|Not recorded|p119|||||||||
12604|Mount Crosby Formation|44510|2|Defined|p252-6,Fig.35|||Overlies unconformably on Blackwall Breccia and Neranleigh-Fernvale Group.||||||
12604|Mount Crosby Formation|44542|2|Defined|p32-34|||=Mount Crosby Insect Shale. Underlies Colleges Conglomerate.||||||
12604|Mount Crosby Formation|44687|6|Mentioned|p227|||Disconformably overlain by Witty Gravel.||||||21-MAR-13
12604|Mount Crosby Formation|44703|14|Not recorded|Map|Late Triassic|Middle Triassic|||||||
12604|Mount Crosby Formation|44705|14|Not recorded|p1,2,5,15|||||||||
12604|Mount Crosby Formation|44708|14|Not recorded|section, Sheet 2||Middle Triassic|||||||
12604|Mount Crosby Formation|44734|14|Not recorded|p5,7,8,15,19|||Pine Mountain area.||||||
12604|Mount Crosby Formation|44775|4|Described|p7,8,map2|Middle Triassic|Early Triassic|||||||
12604|Mount Crosby Formation|44783|14|Not recorded|p16,18|||||||||
12604|Mount Crosby Formation|60726|5|Briefly described|p1-4, p8, throughout text.|Carnian|Carnian|Oldest Formation in the Ipswich Coal Measures. 20-30m thick. Diverse insect fauna (listed).||Lower Ipswich Coal Measures.|||Consists mainly of polymictic, poorly sorted conglomerate but has three shale units, up to 6m thick near the bottom, middle and top of the unit. Upper two shale units are fossiliferous.|
12604|Mount Crosby Formation|67402|5|Briefly described|p222, p223, p225|Carnian|Ladinian|Ipswich Basin. Deposited in an alluvial fan or lacustrine environment.||Kholo Subgroup||Overlain by the Colleges Conglomerate.|Conglomerate, sandstone, siltstone, shale, rhyolitic tuff.|
12604|Mount Crosby Formation|68679|5|Briefly described|p393-395, p435|Late Triassic|Late Triassic|Ipswich Basin. Up to ~90m thick but has significant lateral facies and thickness changes; 21m thick in the type section. Alluvial fan with local swamp/lacustrine environments. Has Carnian plant macrofossils and microfossils.||Kholo Subgroup.||Overlies Sugars Basalt, Weir Basalt and Blackwall Breccia conformably. Is overlain conformably and disconformably by Colleges Conglomerate. Equivalent to Aspley Formation.|Poorly sorted, polymictic cobble conglomerate (with abundant rounded, basement and felsic volcanic clasts), with interbedded shale (locally with abundant fossil insects: species listed), sandstone and two tuff (ignimbrite) horizons.|
12604|Mount Crosby Formation|73450|6|Mentioned|p38||||||||Includes felsic volcanics.|
12633|Mount Devlin Volcanics|35940|5|Briefly described|p637|||||||||
12633|Mount Devlin Volcanics|37612|6|Mentioned|p282|||||||||
12633|Mount Devlin Volcanics|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|||||||
12633|Mount Devlin Volcanics|44000|14|Not recorded|p24,25,27|||Ref. to Reid 1929. Basal unit of Lower Bowen Volcanics in Collinsville area. No longer used.||||||
12633|Mount Devlin Volcanics|44311|14|Not recorded|p195,197|||See also Lexicon.||||||
12633|Mount Devlin Volcanics|44432|14|Not recorded|p44||Permian|||||||
12633|Mount Devlin Volcanics|44571|14|Not recorded|Fig.29|||See also Lexicon.||||||
12633|Mount Devlin Volcanics|48626|14|Not recorded|p21|||See also Lexicon.||||||
12633|Mount Devlin Volcanics|48881|14|Not recorded|p12|||Ref. to Reid 1924-1925,1929. See also Lexicon.||||||
12692|Mount Elliott Slate Member|39496|6|Mentioned|p10|||||||||
12692|Mount Elliott Slate Member|41306|6|Mentioned|p9|||||||||
12692|Mount Elliott Slate Member|44271|2|Defined|p30|||Base of Kuridala Formation Cu deposits.||||||
12692|Mount Elliott Slate Member|44276|14|Not recorded|p11|||||||||
12692|Mount Elliott Slate Member|44290|14|Not recorded|p438||Proterozoic|Unit of Kuridala Formation. (Probably Palaeoproterozoic)||||||
12692|Mount Elliott Slate Member|45166|5|Briefly described|p24|||See also P75||||||
12698|Mount Etna Limestone|31502|5|Briefly described|p94|||Devonian corals. See also P95. Late Siegenian||||||
12698|Mount Etna Limestone|31503|6|Mentioned|p2|||||||||
12698|Mount Etna Limestone|33329|6|Mentioned|p119|||Emsian. Corals.||||||
12698|Mount Etna Limestone|34509|6|Mentioned|p293|||||||||
12698|Mount Etna Limestone|40623|5|Briefly described|p85|||||||||
12698|Mount Etna Limestone|43461|14|Not recorded|Table p618||Emsian|||||||
12698|Mount Etna Limestone|43523|14|Not recorded|p432,433|||||||||
12698|Mount Etna Limestone|43525|14|Not recorded|p130, Table p131|||||||||
12698|Mount Etna Limestone|43526|14|Not recorded|p558||Early Devonian|Contains Acanthophyllum at Silverwood. At least Coblenzian in age||||||
12698|Mount Etna Limestone|43530|14|Not recorded|p1026,1033,1035|Emsian|Siegenian|||||||
12698|Mount Etna Limestone|43532|14|Not recorded|p213||Devonian|Revision of Mictophyllum. See also Lexicon||||||
12698|Mount Etna Limestone|43547|14|Not recorded|p161|||||||||
12698|Mount Etna Limestone|44091|14|Not recorded|Tb.3,p46||Early Devonian|||||||
12698|Mount Etna Limestone|44432|14|Not recorded|p27,28,30||Early Devonian|||||||
12698|Mount Etna Limestone|61761|6|Mentioned|p4|||Of Mount Holly Formation.||||||07-FEB-11
12698|Mount Etna Limestone|73143|6|Mentioned|p11|Pragian|Pragian|Contains Heliolites daintreei tabulate coral (Jones and Hill, 1940).||||||
12714|Mount Formartine Granite|22497|4|Described|p110|||Mount is written Mt in text||||||
12714|Mount Formartine Granite|23423|4|Described|p311 Table 7.4||Early Permian|S-type granite. Also see p244. Mount Formartine Supersuite. Hodgkinson Province.||||||
12714|Mount Formartine Granite|23497|6|Mentioned|p28|||Intrudes Hodgkinson Fm. Age: U-Pb (Shrimp) 357+/-6 Ma.||||||
12714|Mount Formartine Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 394. S-Type.||||||
12714|Mount Formartine Granite|42625|5|Briefly described|Map legend|Triassic|Late Permian|Reserved as Mount Formartine Basalt.||||||
12714|Mount Formartine Granite|42658|4|Described|p37|||||||||
12714|Mount Formartine Granite|42810|2|Defined|Table 1 P16|Early Triassic|Late Permian|see also p27.||||||22-APR-09
12714|Mount Formartine Granite|43259|4|Described|Appendix 1,p44.||Permian|Deformation age of 247+/-2 Ma.||||||
12714|Mount Formartine Granite|43285|5|Briefly described|Map Legend||Early Permian|||||||
12714|Mount Formartine Granite|43625|4|Described|p57,127,Appendix 7|||||||||
12714|Mount Formartine Granite|50387|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Hodgkinson Province. Age: 357 +/- 6 Ma (SHRIMP)||||||11-JUN-04
12714|Mount Formartine Granite|62371|6|Mentioned|p471|Late Devonian|Late Devonian|Part of the Mount Formartine Supersuite. Age: 357+/-6 ma (SHRIMP U-Pb). Mount is Mt in text.||||||26-JUL-06
12714|Mount Formartine Granite|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Hodgkinson Province.||||||
12714|Mount Formartine Granite|68576|5|Briefly described|Q_11: p3-5|||Macalister Range and Ellis Beach areas. A K-Ar age of 247 Ma records post-deformation (D4) uplift and cooling.|357 +/- 6 Ma (SHRIMP: Zucchetto et al.).|||Intrudes Hodgkinson Formation.|Extensively foliated.|
12714|Mount Formartine Granite|69592|5|Briefly described|p241-242|||Cairns. This age is interpreted to reflect metamorphic overprinting by Hunter-Bowen tectonism.|247 +/- 2 Ma (K-Ar: Willmott et al., 1988).|||Intrudes the Hodgkinson Formation.||
12714|Mount Formartine Granite|70033|4|Described|p2 Tb.i, p3 Fig i, p5, p51-57|Late Devonian|Late Devonian|Hodgkinson Province. Interpreted emplacement age (SHRIMP U-Pb zircon) for the pluton at Trinity Beach (this report). Sample lithology is biotite-granite. Other U-Pb zircon (SHRIMP) ages are: 357 +/- 6 Ma (Zucchetto et al. 1999) for pluton in Ellis Beach area, interpreted as emplacement age; and, 382.9 +/- 12 Ma (Zucchetto 1999; cited by Henderson and Donchak, 2013, p242) for pluton in Clohesy River area, interpreted as representing inheritance.|375.2 +/- 1.9 Ma magmatic crystallisation age|||Intrudes Hodgkinson Formation.|Deformed muscovite-biotite granitoid.|
12714|Mount Formartine Granite|70207|5|Briefly described|p4, p11, p59-71, p74, p112||Late Devonian|Part of the Pama Igneous Association, Mossman Orogen. Comprises several small, discrete plutons. Previous age determinations detailed and discussed. Emplacement ages of two discrete plutons. Minimum age given in text as Early Carboniferous?.|376+/-3 Ma; 378.8+/-2.7 Ma (Kositcin et al., 2015)|||Intrudes Hodgkinson Formation.|Brown to brownish-grey, biotite-muscovite granite recrystallised to fine, even-grained aggregate of quartz, feldspars and phyllosilicates. Moderately to intensely deformed granite; local mylonitic foliation.|
12714|Mount Formartine Granite|70345|6|Mentioned|p3, p6-7, p49, p56|Late Devonian|Late Devonian|Is the only known late Devonian igneous unit in or near the Hodgkinson Province.|~375-380 Ma (Emplacement ages)|||Intrudes the Hodgkinson Formation.||
12714|Mount Formartine Granite|70673|5|Briefly described|p5, p7, p87|Late Devonian|Late Devonian|Possible source of some detrital zircons in Hodgkinson Formation. Age range from three discrete intrusions. Shown as Late Devonian-Early Carboniferous? on p7.|380-375 Ma (Kositcin et al., 2015).|||Intrudes Hodgkinson Formation.||
12714|Mount Formartine Granite|71592|5|Briefly described|Appendix A.|||Hodgkinson Province, Mossman Orogen.|376+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite, granite.|
12714|Mount Formartine Granite|72983|6|Mentioned|p15, p80|Famennian|Frasnian|Cairns region.|376.0 +/- 3.0 Ma|||||
12715|Mount Formartine Supersuite|22497|4|Described|p110|Late Devonian|Late Devonian|||||||
12715|Mount Formartine Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
12715|Mount Formartine Supersuite|23423|4|Described|p311 Table 7.4||Early Permian|S-type granite. Intrudes Hodgkinson Formation. Also see p243-244. Comprises one unit - Mount Formartine Granite. Hodgkinson Province.||||||
12715|Mount Formartine Supersuite|23430|5|Briefly described|p493|||S-Type Granites, Daintree Subprovince. Kennedy Province.||||||
12715|Mount Formartine Supersuite|42658|4|Described|p37|||Not a variation on Mount Formartine Granite.||||||
12715|Mount Formartine Supersuite|43625|4|Described|p57|||||||||
12715|Mount Formartine Supersuite|60425|3|Fully described|p35-36, p56 Tb. 4|Late Devonian|Late Devonian|Comprises only one unit, Mount Formartine Granite. Age: 357+/-6Ma (SHRIMP). Intruded Hodgkinson Formation. Detailed lithology included for this muscovite-biotite granite. S-type.||||||07-FEB-11
12715|Mount Formartine Supersuite|62371|5|Briefly described|p472 Fig.3|Devonian|Devonian|Includes Mount Formartine Granite. Age: 357+/-6 Ma (Zuchetto et al., 1999). Mount is Mt in text of figure.||||||09-JUN-06
12715|Mount Formartine Supersuite|63140|6|Mentioned|p572 fig 3|||[New name]. Hodgkinson Province.|357 +/- 6 Ma (Zucchetto et al. 1999).||||S-type.|
12715|Mount Formartine Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Devonian|Late Devonian|Geological province: Hodgkinson Province. S-type granites. Mount is Mt in text of figure.||||||
12715|Mount Formartine Supersuite|69030|5|Briefly described|p6|Devonian|Devonian|Palmer-Barron Subprovince, Hodgkinson Province.|375 +/- 1.9 Ma (SHRIMP).||||S-type granitoids.|
12715|Mount Formartine Supersuite|69592|5|Briefly described|p230, p239, p242, p246, p278, p297-298|Mississippian|Mississippian|Bultitude and Champion (1992). Palmer-Barron Subprovince, along the coast N of Cairns. Plutons are pervasively foliated and elongate parallel to the NW trend of the rocks they intrude; interpreted as syn-tectonic (Tabberabberan Orogeny). Age determinations discussed.|357 +/- 6 Ma (Zucchetto et al., 1999).|||Intrudes Hodgkinson Formation.|Medium-grained, grey biotite-muscovite mozogranite commonly showing blue, strained quartz.|
12733|Mount Gayndah complex|40479|6|Mentioned|p33|||||||||
12733|Mount Gayndah complex|40954|6|Mentioned|p133|||||||||
12745|Mount Gibson Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 312 +/- 4Ma, Rb-Sr.||||||
12745|Mount Gibson Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 296. I-Type.||||||
12745|Mount Gibson Microgranite|40743|6|Mentioned|p318|||||||||
12745|Mount Gibson Microgranite|41824|6|Mentioned|p201|||||||||
12745|Mount Gibson Microgranite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
12745|Mount Gibson Microgranite|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Ages: 310Ma, 310+/-13Ma, 312+/-4Ma (Rb-Sr). Pink to grey, fine-grained, slightly porphyritic biotite granite. I-type.||||||07-FEB-11
12745|Mount Gibson Microgranite|72297|5|Briefly described|p759|||Topaz is recovered from this unit near Innot Hot Springs, northern QLD.||||Intrudes Hodgkinson Formation.||
12754|Mount Godkin Granite|22722|6|Mentioned|p276|||Mount spelled Mt in text||||||
12754|Mount Godkin Granite|24197|5|Briefly described|p32, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1740Ma. Table numbered incorrectly as Tb. 1.1.||||||13-SEP-12
12754|Mount Godkin Granite|24259|6|Mentioned|p107 Fig. 1|||Geological Province: Mount Isa Block.||||||
12754|Mount Godkin Granite|42781|5|Briefly described|p433|||see also Fig.5 p431||||||11-MAY-18
12754|Mount Godkin Granite|50332|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of the Burstall Suite. Age: 1760-1720Ma. Intruded into the Kalkadoon-Ewen Province and Eastern Fold Belt Province. Geological Province: Kalkadoon-Ewen Province and Eastern Fold Belt Province.||||||02-JUN-16
12754|Mount Godkin Granite|50536|5|Briefly described|p1.4, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Burstall Suite.||||||07-NOV-08
12754|Mount Godkin Granite|63866|5|Briefly described|p60|||Wonga Belt.||||||
12754|Mount Godkin Granite|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Granite.|
12754|Mount Godkin Granite|69056|5|Briefly described|p14 Tb.3, p18, p23, p28|||Wonga Event-aged. Modelling values listed.||Burstall Suite.|||A multiphase intrusive consisting of granite, quartz diorite and quartz monzonite, altered endoskarn-bearing metagranite, aplite and microgranite and leucogranite and pegmatite.|
12754|Mount Godkin Granite|69591|6|Mentioned|p60|||||Burstall Suite.|||Granite.|
12754|Mount Godkin Granite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|The four facies are mapped separately.|||||Leucogranite and pegmatite; granophyric microgranite and aplite; altered endoskarn-bearing metagranite; quartz diorite and quartz monzonite.|
12754|Mount Godkin Granite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|The four facies are mapped separately.|||||Leucogranite and pegmatite; granophyric microgranite and aplite; altered endoskarn-bearing metagranite; quartz diorite and quartz monzonite.|
12754|Mount Godkin Granite|70532|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Pink, fine- to medium-grained hornblende syenogranite to monzogranite, commonly with granophyric textures; local biotite syenogranite. Separately mapped: granophyric microgranite and aplite; altered endoskarn-bearing metagranite.|
12754|Mount Godkin Granite|70574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes two unnamed members: altered endoskarn bearing metagranite; granophyric microgranite and aplite.|||Includes two unnamed members.||Fine-medium grained hornblende syenogranite to monzogranite, commonly with granophyric textures; local biotite syenogranite.|
12754|Mount Godkin Granite|72799|4|Described|p1, p3, p10, p34-38|Statherian|Statherian|Geochron is a new magmatic crystallisation age. Forms a prominent, topographically high range ca 45 km northwest of Cloncurry; has a distinct ellipsoid mapped extent.|1739 +/- 3 Ma SHRIMP U-Pb|Burstall Suite||Intrudes Corella Formation. Coeval with Burstall Granite and Lunch Creek Gabbro.|Heterogeneous with microgranite, granophyric granite, granodiorite, different types of gabbro, breccia and extensive rafts/remnants of Corella Formation observed locally. Mostly altered endoskarn-bearing metagranite.|
12754|Mount Godkin Granite|73529|6|Mentioned|p2 Fig.1, p14|||Sill-like magmatic body, folded during Isan Orogeny.||Burstall Suite||||
12754|Mount Godkin Granite|73553|4|Described|p71, p122, p126-135, p142, p144, p205|Statherian|Statherian|Mary Kathleen Domain. Burstall Igneous Subprovince. Included in the Burstall Granite in early 1-100 000 scale mapping. More recently divided as a distinct unit with five subunits (Withnall et al., 2015, 2016) after detailed mapping (Oliver et al., 1991). Area was described by Derrick et al., (1971; 1978), Wilson et al., (1979) and Oliver et al., (1991). Cogenetic with Burstall Granite. Relatively low magnetic response in most parts, with bands of local higher response. Main body has white to bluish tones on radiometric images, pinker to the north.|1739+/-3 Ma U-Pb zircon (SHRIMP)|Burstall Suite||Intrudes Corella Formation, Lime Creek Metabasalt|Heterogeneous, includes altered endoskarn-bearing metagranite, granophyric microgranite and aplite, fine to medium-grained hornblende syenogranite to monzogranite, quartz diorite and quartz monzonite, leucogranite and pegmatite, gabbro.|
12768|Mount Guide Quartzite|22644|5|Briefly described|5|||Geol province: Mt Isa Basin.  Mount as 'Mt' in text||||||01-FEB-07
12768|Mount Guide Quartzite|23031|6|Mentioned|24|||||||||
12768|Mount Guide Quartzite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Contains the May Downs Gneiss Member. Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
12768|Mount Guide Quartzite|23395|5|Briefly described|p395|||||||||
12768|Mount Guide Quartzite|23466|5|Briefly described|p265|||||||||
12768|Mount Guide Quartzite|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
12768|Mount Guide Quartzite|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|Mount is Mt. in text.||||||07-NOV-08
12768|Mount Guide Quartzite|24419|5|Briefly described|p16, p12 Fig. 4|Proterozoic|Proterozoic|Of the lower part of the  Haslingden Group. Includes Yappo Member in lower section; upper section (unnamed) of ridge-forming quartz-rich sandstone metamorphosed to quartzite.Conformably overlain by Eastern Creek Volcanics.See also p13 Fig. 5, p15 Fig. 6.||||||
12768|Mount Guide Quartzite|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Bottletree Formation. Overlain by Eastern Creek Volcanics.||||||
12768|Mount Guide Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.  Overlain by Eastern Creek Volcanics.||||||25-AUG-04
12768|Mount Guide Quartzite|30530|6|Mentioned|p515|||||||||
12768|Mount Guide Quartzite|30534|3|Fully described|p300|||||||||
12768|Mount Guide Quartzite|30536|6|Mentioned|p100|||Refers Stratigraphy||||||
12768|Mount Guide Quartzite|30723|6|Mentioned|p340|||Maximum age 1785 my||||||
12768|Mount Guide Quartzite|30725|5|Briefly described|p574|||||||||
12768|Mount Guide Quartzite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12768|Mount Guide Quartzite|32041|6|Mentioned|p352|||||||||
12768|Mount Guide Quartzite|32660|5|Briefly described|Table 5|||||||||
12768|Mount Guide Quartzite|32951|6|Mentioned|Table 1|||||||||
12768|Mount Guide Quartzite|32959|6|Mentioned|Fig.21|||||||||
12768|Mount Guide Quartzite|33214|5|Briefly described|p1279|||Age discussed.||||||15-MAR-18
12768|Mount Guide Quartzite|33893|5|Briefly described|p30|||See also Table 1 & p27.||||||15-MAR-18
12768|Mount Guide Quartzite|33894|6|Mentioned|Table 2|||||||||
12768|Mount Guide Quartzite|33896|6|Mentioned|p468|||||||||
12768|Mount Guide Quartzite|33897|6|Mentioned|p1280|||||||||
12768|Mount Guide Quartzite|33900|4|Described|p10|||Mention p7||||||15-MAR-18
12768|Mount Guide Quartzite|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|34499|6|Mentioned|Table 1|||Rock types Table 11||||||
12768|Mount Guide Quartzite|35074|6|Mentioned|Fig.2|||||||||
12768|Mount Guide Quartzite|35139|6|Mentioned|p41|||||||||
12768|Mount Guide Quartzite|35286|6|Mentioned|Fig.17|||||||||
12768|Mount Guide Quartzite|35295|6|Mentioned|Fig.2|||||||||
12768|Mount Guide Quartzite|35369|6|Mentioned|Table 1|||Stratigraphy||||||
12768|Mount Guide Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12768|Mount Guide Quartzite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12768|Mount Guide Quartzite|37459|6|Mentioned|p423|||||||||
12768|Mount Guide Quartzite|37568|5|Briefly described|p81|||||||||
12768|Mount Guide Quartzite|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|37862|6|Mentioned|p581|||||||||
12768|Mount Guide Quartzite|38232|6|Mentioned|p83|||||||||
12768|Mount Guide Quartzite|38234|6|Mentioned|p103|||||||||
12768|Mount Guide Quartzite|38276|6|Mentioned|Fig.1|||||||||
12768|Mount Guide Quartzite|38350|4|Described|p9|||||||||
12768|Mount Guide Quartzite|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Haslingden Group. Contains the Yappo Member. Underlies the Eastern Creek Volcanics.||||||01-SEP-08
12768|Mount Guide Quartzite|38560|6|Mentioned|p114|||||||||
12768|Mount Guide Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12768|Mount Guide Quartzite|38834|6|Mentioned|p162|||||||||
12768|Mount Guide Quartzite|39362|6|Mentioned|Fig.1|||||||||
12768|Mount Guide Quartzite|39445|5|Briefly described|Table 2|||See also p40.||||||15-MAR-18
12768|Mount Guide Quartzite|39622|6|Mentioned|p21|||||||||
12768|Mount Guide Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12768|Mount Guide Quartzite|40221|6|Mentioned|p6|||||||||
12768|Mount Guide Quartzite|40598|6|Mentioned|Fig.2|||||||||
12768|Mount Guide Quartzite|40623|5|Briefly described|p95|||||||||
12768|Mount Guide Quartzite|40840|6|Mentioned|Map legend|||||||||
12768|Mount Guide Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
12768|Mount Guide Quartzite|41978|6|Mentioned|p501|||||||||
12768|Mount Guide Quartzite|41979|6|Mentioned|Fig.2 P512|||||||||
12768|Mount Guide Quartzite|42503|5|Briefly described|p336|||||||||
12768|Mount Guide Quartzite|42523|4|Described|p372|||||||||
12768|Mount Guide Quartzite|42565|5|Briefly described|Table 1 P5|||||||||
12768|Mount Guide Quartzite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Haslingden Group. Sandstone in upper part; greywacke and conglomerate in lower part.||||||09-FEB-09
12768|Mount Guide Quartzite|42818|5|Briefly described|Fig.2 P205|||Of Haslingden Group.||||||01-SEP-08
12768|Mount Guide Quartzite|43608|6|Mentioned|Fig.11,p11|||||||||
12768|Mount Guide Quartzite|44195|6|Mentioned|p356 Fig.9|||||||||
12768|Mount Guide Quartzite|44210|2|Defined|Tb.1,map,p8,11|||||||||
12768|Mount Guide Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|44271|2|Defined|p33,53|||||||||
12768|Mount Guide Quartzite|44273|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|44275|14|Not recorded|Map Legend|||||||||
12768|Mount Guide Quartzite|44276|2|Defined|p10,15,17,Tb.1,map|||||||||
12768|Mount Guide Quartzite|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|44278|2|Defined|p7,Tb.1,map|||||||||
12768|Mount Guide Quartzite|44517|14|Not recorded|p234,235|||||||||
12768|Mount Guide Quartzite|44521|14|Not recorded|p37,map|||||||||
12768|Mount Guide Quartzite|44749|14|Not recorded|p25,26|||Discussion on age of Kalkadoon Granite.||||||
12768|Mount Guide Quartzite|44755|14|Not recorded|Fig.1,p90,93||Mesoproterozoic|||||||
12768|Mount Guide Quartzite|44765|14|Not recorded|p15,16||Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|44766|14|Not recorded|p23-25|||Suggests that Kalkadoon Granite is younger than Mount Guide Quartzite.||||||
12768|Mount Guide Quartzite|44806|14|Not recorded|p283|||||||||
12768|Mount Guide Quartzite|44812|14|Not recorded|p6|||Soil.||||||
12768|Mount Guide Quartzite|44989|2|Defined|p.65-7|||Tb.III. On many pages. Overlies Argylla Formation & Leichhardt Metamorphics; Underlies conf. Eastern Creek Volcanics. 4,000-8,0000+ '. (F54-1,2,5,6).||||||
12768|Mount Guide Quartzite|45136|3|Fully described|p45|||Also mention p19.||||||15-MAR-18
12768|Mount Guide Quartzite|45161|4|Described|p23|||||||||
12768|Mount Guide Quartzite|45166|4|Described|p14|||||||||
12768|Mount Guide Quartzite|45287|14|Not recorded|p.225,226||Paleoproterozoic|Contemp.with Ballara & Leander Quartzites.||||||07-NOV-08
12768|Mount Guide Quartzite|46801|6|Mentioned|p115|||See also Fig. 14||||||
12768|Mount Guide Quartzite|46859|4|Described|p312|||Mention p311.||||||15-MAR-18
12768|Mount Guide Quartzite|46962|4|Described|Table 1|||See also Fig.3.||||||
12768|Mount Guide Quartzite|46976|6|Mentioned|p98|||||||||
12768|Mount Guide Quartzite|46996|6|Mentioned|p273|||||||||
12768|Mount Guide Quartzite|49009|6|Mentioned|p8|||||||||
12768|Mount Guide Quartzite|49041|6|Mentioned|Table 4|||||||||
12768|Mount Guide Quartzite|50100|5|Briefly described|p16-17|Proterozoic|Proterozoic|Of the lower Haslingden Group. Includes the Yappo Member. Conformably overlain by the Eastern Creek Volcanics. Intruded by Garden Creek Porphyry.  Geological Province: Western Fold Belt Province.||||||11-FEB-09
12768|Mount Guide Quartzite|50332|5|Briefly described|p17|Proterozoic|Proterozoic|Of the lower Haslingden Group. Overlain comformably by Myally Subgroup. Includes; Yappo Member.||||||07-FEB-11
12768|Mount Guide Quartzite|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
12768|Mount Guide Quartzite|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
12768|Mount Guide Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Haslingdon Group. Includes: Yappo Member.||||||
12768|Mount Guide Quartzite|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
12768|Mount Guide Quartzite|61204|5|Briefly described|p538|||Geological Province: Mount Isa Inlier. Of the Haslingden Group. Coarse sandstone and lesser quartzite.||||||
12768|Mount Guide Quartzite|61922|5|Briefly described|p8, p9 Fig. 3, p20 Fig.12.|||Older component of immature greywacke type clastic or sericitic sandstone; and, younger component of mature, white, fine- to medium-grained quartz sandstone. Geol. Prov: Mount Isa Inlier/Western Fold Belt.||||||
12768|Mount Guide Quartzite|61923|5|Briefly described|p29 Fig.2|||Geological Province: Mount Isa Inlier.||||||
12768|Mount Guide Quartzite|61929|5|Briefly described|p128 Fig. 2|||||||||
12768|Mount Guide Quartzite|61936|5|Briefly described|p193|||Shallow marine clastic successions. Geological Province: Leichhardt Superbasin, Eastern Fold Belt, Mount Isa Inlier. Mount is Mt in text.||||||
12768|Mount Guide Quartzite|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: >1785Ma. Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
12768|Mount Guide Quartzite|62873|5|Briefly described|p692|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group. Coarse sandstone (lesser quartzite). Geological Province: Mount Isa Inlier.||||||07-NOV-08
12768|Mount Guide Quartzite|62988|5|Briefly described|p34|||Included in the Guide Supersequence spanning ~1800-1785Ma in age. Geological Province: Mount Isa Inlier.||||||25-JAN-07
12768|Mount Guide Quartzite|63023|5|Briefly described|p1025 Fig. 2|||Of Haslingden Group. Geological Province: Leichardt Superbasin. Divided into 'upper' and 'lower' sections. Mount may be Mt in text. This unit together with Bottletree Formation form the Guide Supersequence.||||||
12768|Mount Guide Quartzite|63109|6|Mentioned|p1111, p1108 Fig. 3, p1112|||Mount is Mt in text. Proximal fluvial sandstone. Geological Province: Leichhardt Superbasin.||||||30-SEP-08
12768|Mount Guide Quartzite|63111|5|Briefly described|p1162, p1163 Fig. 3|Statherian|Statherian|Overlain by Eastern Creek Volcanics, underlain by Bottletree Formation. Proximal fluvial facies associated rocks composed of poorly sorted and immature, corse-to fine grained sandstone, pebbly sandstone + conglomerate. Geol Prov: Leichhardt Superbasin.||||||07-FEB-11
12768|Mount Guide Quartzite|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Appears as Mt Guide Qtz in Fig.2, and as Mount Guide Sandstone in Fig.13.||Of the Haslingden Group||Overlies Bottle Tree Formation. Is overlain by Eastern Creek Volcanics.||
12768|Mount Guide Quartzite|63114|6|Mentioned|p1253 Fig.2, p1269-1270. |||Possible aquifer in the Mount Isa basin.||||Overlies Bottletree Formation. Is overlain by Eastern Creek Volcanics.|Includes proximal fluvial siliciclastic facies.|
12768|Mount Guide Quartzite|63115|6|Mentioned|p1275, p1279, p1282-1283, p1290. |||Base of Leichhardt superbasin. Potential aquifer sequence. Appears as Mount Guide Sandstone in Fig.4.|||||Sandstones and conglomerates.|
12768|Mount Guide Quartzite|63116|6|Mentioned|p1299 Tb.1, p1300-1306, p1309 |||Leichhardt superbasin. Appears as Mount Guide Sandstone in Fig.2. Material properties detailed. Aquifer.||||||
12768|Mount Guide Quartzite|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. 6000m thick.|||||Sandstone, greywacke, arkose, grit.|
12768|Mount Guide Quartzite|63866|5|Briefly described|p58|Statherian|Statherian|Leichhardt Superbasin. Numeric ages are dates of maximum deposition and derived from Neumann et al., 2006.|1793 +/- 9 Ma and 1773 +/- 19 Ma|Guide Supersequence||||
12768|Mount Guide Quartzite|64250|5|Briefly described|p16 fig 6, p11 fig 3, p19, p21, p22|||Western Fold Belt, Mount Isa Inlier.|<1773 +/- 16 Ma|Haslingden Group|||Siliciclastics; minor basalt.|
12768|Mount Guide Quartzite|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Basal unit of Eastern Creek Volcanics. Age: ca.1785Ma.||||||07-FEB-11
12768|Mount Guide Quartzite|64744|6|Mentioned|p353 Fig.4. |Statherian||Mount Isa Basin.||||||
12768|Mount Guide Quartzite|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group. Age: ca.1785Ma. Geological Province: Mt Isa Inlier. Coarse sandstone and minor quartzite.||||||07-FEB-11
12768|Mount Guide Quartzite|64834|5|Briefly described|p13 Fig.2, p33 Fig.14, p35-36|||Leichhardt Superbasin. Western Succession of Mount Isa Basin. Shown as Mt Guide Quartzite. Refers often to lower portion of Mount Guide Quartzite with regards to U and fluids.|||||Conglomerate, with cobble bed near base, and sandstone.|
12768|Mount Guide Quartzite|65396|5|Briefly described|p16, p82, p175, p187, p190, p192|Statherian|Statherian|See also p194-195, p241. Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough. Detrital zircon sources listed.|<1793 +/- 1 Ma|Haslingden Group||Overlies Bottletree Formation; overlain by Eastern Creek Volcanics.|Quartzite/sandstone with minor basalt.|
12768|Mount Guide Quartzite|66529|5|Briefly described|p32, p34  |||Leichhardt Superbasin rift fill. Hosts some uranium prospects.||||Is overlain by Eastern Creek Volcanics.|Shallow-marine siliciclastics and volcanic rocks.|
12768|Mount Guide Quartzite|66824|6|Mentioned|p133, 135|||||||Is overlain by Eastern Creek Volcanics.||
12768|Mount Guide Quartzite|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||Unit in Haslingden Group.||||
12768|Mount Guide Quartzite|67323|4|Described|GIS attrib tbl, p9, p13, p31, p39|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Leichhardt River Domain, Mount Isa Inlier. Marine facies. Maximum depositional age: 1773 +/- 16 Ma (Neumann et al 2006).|~1780 Ma.|Lower Haslingden Group.|Includes Yappo Member.|Correlated with Westmoreland Conglomerate and Wire Creek Sandstone.|Quartzite, feldspathic and micaceous quartzite, minor gneiss.|
12768|Mount Guide Quartzite|67499|6|Mentioned|p938, p941|||||Of the Haslingden Group.|||Coarse sandstone.|
12768|Mount Guide Quartzite|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Part of Guide Supersequence, Leichhardt Superbasin, Western Succession.||||Overlies Bottletree Formation, unconfomably overlain by Eastern Creek Volcanics.||
12768|Mount Guide Quartzite|68575|5|Briefly described|p97|||Maximum depositional age.|1793 +/- 9 Ma (Neumann et al., 2007).|||Is overlain by Eastern Creek Volcanics.||
12768|Mount Guide Quartzite|68732|5|Briefly described|p160, p161, p165 Fig.3|Statherian|Orosirian|Shoreline facies deposited above fair-weather wave base. Shown as both upper and lower Mount Guide Quartzite. Of the Guide Supersequence. Maximum sedimentary depositional ages.|1773 +/ 16 Ma (upper); 1793 +/- 9 Ma (lower)|Of the Haslingden Group.|||Fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|01-DEC-17
12768|Mount Guide Quartzite|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|Statherian|Statherian|Leichhardt River Fault Trough. Part of a thick rift-sag sequence.||||Overlies Bottletree Formation, overlain by Eastern Creek Volcanics||09-FEB-18
12768|Mount Guide Quartzite|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||Unit in Haslingden Group.||Overlies Bottletree Formation.||25-JAN-19
12768|Mount Guide Quartzite|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||||||
12768|Mount Guide Quartzite|69591|4|Described|p33-34, p57, p103, p105|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of the Guide Supersequence. Fluvial to tide-dominated shelf deposits. Age by Neumann and Fraser (2007); an age of 1793 +/- 9 Ma is also given.|1773 +/- 16 Ma (maximum depositional age).|Haslingden Group.||Overlies Bottletree Formation. Equivalent to Leander Quartzite. Correlated with Westmoreland Conglomerate.|Quartzite, feldspathic and micaceous quartzite, minor gneiss.|
12768|Mount Guide Quartzite|70282|6|Mentioned|p544 Tb.1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||Overlies Bottletree Formation, overlain by Eastern Creek Volcanics||13-FEB-18
12768|Mount Guide Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1793+/-9 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
12768|Mount Guide Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||||Overlies Bottletree Formation and underlies Eastern Creek Formation.||
12768|Mount Guide Quartzite|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group|Includes Yappo Member.|Shown as younger than Bottletree Formation. Underlies Eastern Creek Volcanics.|Quartzite, feldspathic and micaceous quartzite, minor gneiss. Pebbly greywacke to conglomerate, minor quartzite, feldspathic sandstone and metabasalt, greywacke, quartzite and feldspathic sandstone.|
12768|Mount Guide Quartzite|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group|Includes Yappo Member.|Shown as younger than Bottletree Formation. Underlies Eastern Creek Volcanics.|Quartzite, feldspathic and micaceous quartzite, minor gneiss. Pebbly greywacke to conglomerate, minor quartzite, feldspathic sandstone and metabasalt, greywacke, quartzite and feldspathic sandstone.|
12768|Mount Guide Quartzite|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Orosirian|Part of the Leichhardt Superbasin. Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Guide Supersequence||Partially overlies Bottletree Formation and overlain by Eastern Creek Volcanics.||16-MAR-21
12768|Mount Guide Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||Overlain by Eastern Creek Volcanics. Partly underlain by Bottletree Formation.||
12768|Mount Guide Quartzite|73083|6|Mentioned|p53|||||||||
12768|Mount Guide Quartzite|73525|5|Briefly described|p2 Fig.1, p4-5 Fig.2, p19 Fig.13|Statherian|Statherian|Misspelt as Quarzite. Leichhardt River Domain.|1773+/-16 Ma, 1793+/-9 Ma maximum depositional age||||Siliciclastics.|
12790|Mount Hedlow Trachyte|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Kih].  Trachyte plugs, basalt flows.||||||
12790|Mount Hedlow Trachyte|31658|6|Mentioned|Map legend|Late Cretaceous|Late Cretaceous|||||||
12790|Mount Hedlow Trachyte|31659|4|Described|p76|||Cretaceous||||||
12790|Mount Hedlow Trachyte|32358|4|Described|p20|||||||||
12790|Mount Hedlow Trachyte|33879|6|Mentioned|p287|||||||||
12790|Mount Hedlow Trachyte|34408|6|Mentioned|p185|||On Table||||||
12790|Mount Hedlow Trachyte|35007|6|Mentioned|p77|||||||||
12790|Mount Hedlow Trachyte|37607|6|Mentioned|p339|||||||||
12790|Mount Hedlow Trachyte|37860|6|Mentioned|p571|||||||||
12790|Mount Hedlow Trachyte|39445|5|Briefly described|Table 14|||||||||
12790|Mount Hedlow Trachyte|41246|6|Mentioned|Map legend|Cretaceous||||||||
12790|Mount Hedlow Trachyte|41576|4|Described|p20|||See also Table 1||||||
12790|Mount Hedlow Trachyte|41577|6|Mentioned|Map legend|Late Cretaceous||||||||
12790|Mount Hedlow Trachyte|41922|4|Described|Table 2, P12|||||||||
12790|Mount Hedlow Trachyte|41931|5|Briefly described|p96|||||||||
12790|Mount Hedlow Trachyte|50212|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
12790|Mount Hedlow Trachyte|60557|5|Briefly described|p18 Fig. 5a, p28|Cretaceous|Cretaceous|||||||
12790|Mount Hedlow Trachyte|65668|6|Mentioned|p25-26|Late Cretaceous|Late Cretaceous|NE of Rockhampton. Overlies basalt; erroneously correlated with Mount Salmon Volcanics W of Rockhampton, which also overlie basalts but which have been dated as Early Cretaceous.||||||
12790|Mount Hedlow Trachyte|68008|3|Fully described|p225, p250-251, p253, p255, p259|Late Cretaceous|Late Cretaceous|See also p266-270, p294, p463-465, p493, p531. Kirkegaard et al. (1966, 1970), for a series of felsic plugs described by Jardine (1923). Comprises 19 small plugs between Rockhampton and Yeppoon. Forms domes, headlands and islands. Up to 393m height. Geophysics described. Geochemistry detailed; similarities with Wycarbah Volcanics and Alton Downs Basalt.  U-Pb zircon ages by Sutherland et al. (1996). Various other ages given; Harding (1969) obtained a K-Ar whole rock age of 71 Ma. Assumed to form a bimodal assemblage with Alton Downs Basalt.|80 +/- 3 Ma and 73 +/- 3 Ma.|||Intrudes Wandilla Formation , Balnagowan Volcanic Member, Jim Crow beds. Surrounded by Alton Downs Basalt.|Predominantly rhyolite (60%) and trachyte. Rhyolite is fine-grained and grey. Trachyte is fine-grained, grey to off-white. Two basalt plugs have been included in this unit.|
12790|Mount Hedlow Trachyte|69594|5|Briefly described|p552, p559, p565|Late Cretaceous|Late Cretaceous|Intrudes the Jim Crow Basin. Within-plate igneous activity. Has similarities with Dalma Basalt.|80 - 73 +/- 3 Ma (SHRIMP: Sutherland et al. 1996).||||Trachyte plugs, basalt flows.|
12790|Mount Hedlow Trachyte|73450|4|Described|p4, p49-51, p53|Campanian|Campanian|Forms a bimodal assemblage with the Alton Downs Basalt. Comprises 18 small bodies between Rockhampton and Yeppoon, and forms coastal exposures between Yeppoon and Kinka Beach; forms prominent rounded domes or plugs. Coherent and autoclastic facies are present. Two basalt plugs have been mapped as subunit Kih/b. Lots of geochronology of various vintages and methods; highlights are U-Pb SHRIMP zircon ages of 73 to 80 +/- 3 Ma (Sutherland et al., 1996) and an unexplained U-Pb TIMS zircon age of 167.8 +/- 0.5 Ma (Murray et al., 2012). [Misspelt as Mount Hedlow Trachyite on p53].|73-80 +/- 3 Ma U-Pb SHRIMP||||Fine grained rhyolite and trachyte with uncommon basalt.|
12792|Mount Hendry Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Early Cambrian|||||||
12792|Mount Hendry Formation|23031|4|Described|30|||Geological  province: Georgina Basin.||||||09-NOV-06
12792|Mount Hendry Formation|23393|5|Briefly described|p23 Fig. 6|Middle Cambrian|Early Cambrian|Mount is Mt. in text of figure.  Geological Province: Georgina Basin.||||||
12792|Mount Hendry Formation|23986|5|Briefly described|p68|||Mount is Mt. in text.||||||
12792|Mount Hendry Formation|30479|6|Mentioned|Fig.7|||Lower Cambrian age||||||
12792|Mount Hendry Formation|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
12792|Mount Hendry Formation|33482|6|Mentioned|p6|||Lower Middle Cambrian||||||
12792|Mount Hendry Formation|35001|6|Mentioned|Fig.45|||||||||
12792|Mount Hendry Formation|35054|6|Mentioned|p246|||||||||
12792|Mount Hendry Formation|36448|6|Mentioned|Fig.1|||||||||
12792|Mount Hendry Formation|38209|5|Briefly described|Fig.1|||||||||
12792|Mount Hendry Formation|38446|6|Mentioned|p144|||||||||
12792|Mount Hendry Formation|39445|5|Briefly described|Table 4|||See also p61 and p62.||||||09-NOV-06
12792|Mount Hendry Formation|39690|6|Mentioned|Table 1|||||||||
12792|Mount Hendry Formation|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
12792|Mount Hendry Formation|40221|4|Described|p19|||Mention p6.||||||09-NOV-06
12792|Mount Hendry Formation|40386|6|Mentioned|Fig.1|||||||||
12792|Mount Hendry Formation|40686|6|Mentioned|Fig.3|||||||||
12792|Mount Hendry Formation|40852|5|Briefly described|p38|||||||||
12792|Mount Hendry Formation|40855|6|Mentioned|Fig.24.1|||||||||
12792|Mount Hendry Formation|40856|6|Mentioned|Fig.23.6|||||||||
12792|Mount Hendry Formation|40858|5|Briefly described|p132|||||||||
12792|Mount Hendry Formation|41129|6|Mentioned|Fig.8|||||||||
12792|Mount Hendry Formation|41240|6|Mentioned|p112|||||||||
12792|Mount Hendry Formation|41388|6|Mentioned|Fig.2|||||||||
12792|Mount Hendry Formation|45079|5|Briefly described|p10|||Recommends term be discontinued. See p16.||||||09-NOV-06
12792|Mount Hendry Formation|47058|6|Mentioned|Fig.4 P124|||||||||
12792|Mount Hendry Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cambrian|Neoproterozoic|Georgina Basin||Narpa Group|||Conglomerate, arenite, arkose, shale, mudstone, dolomite|
12792|Mount Hendry Formation|69591|5|Briefly described|p97, p98 Fig.2.91|Cambrian|Cambrian|Basal clastics of the Georgina Basin.||||Overlain by ?Thorntonia Limestone.||
12822|Mount Isa Group|22453|5|Briefly described|p 11|||NT and QLD||||||
12822|Mount Isa Group|22468|5|Briefly described|p 17|||||||||
12822|Mount Isa Group|22483|6|Mentioned|Table 2 p416.|||||||||
12822|Mount Isa Group|22498|5|Briefly described|Fig2 P235, Fig5|||||||||
12822|Mount Isa Group|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Underlain by Fiery Creek Volcanics.Of the Yaringa Metamorphics. Mount as 'Mt' in text||||||09-NOV-06
12822|Mount Isa Group|22665|6|Mentioned|P219, P227|||Mount actually spelt Mt||||||
12822|Mount Isa Group|22680|6|Mentioned|83|||Mount as 'Mt' in text||||||
12822|Mount Isa Group|22747|6|Mentioned|Table1,p7|||Part of Ploughed Mountain Beds equivalent to Mount Isa Group||||||
12822|Mount Isa Group|22955|6|Mentioned|160||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological province: Leichardt Sub Province.||||||07-NOV-08
12822|Mount Isa Group|23072|6|Mentioned|p754|||||||||
12822|Mount Isa Group|23291|6|Mentioned|p24|||Geological Province: Georgetown Region.||||||08-JUL-15
12822|Mount Isa Group|23313|6|Mentioned|319 Fig. 6|||||||||
12822|Mount Isa Group|23362|6|Mentioned|337|||||||||
12822|Mount Isa Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
12822|Mount Isa Group|23395|6|Mentioned|p383|||Mount is spelt Mt. in text.||||||
12822|Mount Isa Group|23397|5|Briefly described|p463|||Mount is Mt. in text.||||||
12822|Mount Isa Group|23398|4|Described|p454|||||||||
12822|Mount Isa Group|23399|4|Described|p485|||||||||
12822|Mount Isa Group|23408|5|Briefly described|p509, p511, p513 Fig. 2|||Previous interpretations of this group are included. Comprises Surprise Ck. Beds, Warrina Pk Quartzite, Mondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear and Kennedy Siltstones, Magazine Shale (Cavaney 1975).||||||15-JUN-09
12822|Mount Isa Group|23409|5|Briefly described|p536|||Isa Superbasin||||||
12822|Mount Isa Group|23447|5|Briefly described|p436|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|23448|5|Briefly described|p479|Statherian|Statherian|Age: 1670Ma.||||||09-NOV-06
12822|Mount Isa Group|23466|5|Briefly described|p269|||||||||
12822|Mount Isa Group|23518|4|Described|p9 Fig. 3, p12|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
12822|Mount Isa Group|23554|6|Mentioned|pB34|||Geological Province: Mt Isa Inlier.||||||
12822|Mount Isa Group|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin||||||
12822|Mount Isa Group|23957|6|Mentioned|p1123|||||||||
12822|Mount Isa Group|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
12822|Mount Isa Group|23966|5|Briefly described|p1309|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.   Age: 1653 +/- 7Ma.||||||
12822|Mount Isa Group|23969|6|Mentioned|p1371 Fig.2|||Mount is Mt. in text. Geological Province: Mount Isa Inlier.||||||
12822|Mount Isa Group|24254|6|Mentioned|p21|||||||||
12822|Mount Isa Group|24419|5|Briefly described|p14, p17, p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Warrina Park Quartzite (basal unit), Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone. Overlies Surprise Creek Formation.  Geological Province: Isa Superbasin. Equivalent to lower McNamara Group in Lawn Hill Subprovince.||||||07-NOV-08
12822|Mount Isa Group|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Lena Quartzite. Geological Province: Leichardt River Fault Trough.||||||
12822|Mount Isa Group|29969|6|Mentioned|p392|||||||||
12822|Mount Isa Group|30354|6|Mentioned|p9|||Refers to micro palaeontology||||||
12822|Mount Isa Group|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||25-AUG-04
12822|Mount Isa Group|30530|6|Mentioned|p515|||||||||
12822|Mount Isa Group|30531|6|Mentioned|p15|||Also mention P20 and P22.||||||
12822|Mount Isa Group|30534|6|Mentioned|p300|||See also P305||||||
12822|Mount Isa Group|30535|1|Redefined|p404|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|30723|5|Briefly described|p340|||||||||
12822|Mount Isa Group|30724|6|Mentioned|p73|||||||||
12822|Mount Isa Group|30725|5|Briefly described|p574|||||||||
12822|Mount Isa Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|31207|6|Mentioned|p1414|||||||||
12822|Mount Isa Group|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|31421|6|Mentioned|p509|||||||||
12822|Mount Isa Group|31704|6|Mentioned|p5|||Minor Copper in shale association||||||
12822|Mount Isa Group|31821|6|Mentioned|p1023|||||||||
12822|Mount Isa Group|32041|4|Described|p353|||||||||
12822|Mount Isa Group|32042|5|Briefly described|p38|||||||||
12822|Mount Isa Group|32100|6|Mentioned|p273|||||||||
12822|Mount Isa Group|32144|6|Mentioned|p116|||Organic matter||||||
12822|Mount Isa Group|32211|6|Mentioned|p12|||Lower Proterozoic||||||
12822|Mount Isa Group|32376|6|Mentioned|p1541|||||||||
12822|Mount Isa Group|32466|6|Mentioned|p316|||||||||
12822|Mount Isa Group|32479|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|32660|4|Described|Table 5|||||||||
12822|Mount Isa Group|32818|5|Briefly described|p17|||Age||||||
12822|Mount Isa Group|32951|6|Mentioned|Table 1|||||||||
12822|Mount Isa Group|32959|6|Mentioned|p31|||||||||
12822|Mount Isa Group|33111|6|Mentioned|p5|||||||||
12822|Mount Isa Group|33214|5|Briefly described|p1279|||Age discussed||||||
12822|Mount Isa Group|33791|6|Mentioned|p373|||||||||
12822|Mount Isa Group|33893|6|Mentioned|Table 1|||||||||
12822|Mount Isa Group|33894|6|Mentioned|Table 2|||||||||
12822|Mount Isa Group|33896|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|33897|6|Mentioned|p1280|||||||||
12822|Mount Isa Group|33900|4|Described|p13|||Mention p4.||||||09-NOV-06
12822|Mount Isa Group|34499|4|Described|p226|||See Table 11.||||||09-NOV-06
12822|Mount Isa Group|34891|6|Mentioned|p240|||||||||
12822|Mount Isa Group|35001|6|Mentioned|p261|||||||||
12822|Mount Isa Group|35004|6|Mentioned|p266|||||||||
12822|Mount Isa Group|35074|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|35114|6|Mentioned|p199|||||||||
12822|Mount Isa Group|35115|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|35116|4|Described|p181|||See also p177 and Table 4.||||||09-NOV-06
12822|Mount Isa Group|35261|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|35286|6|Mentioned|p158|||||||||
12822|Mount Isa Group|35309|6|Mentioned|p373|||||||||
12822|Mount Isa Group|35369|6|Mentioned|PB5|||||||||
12822|Mount Isa Group|35495|6|Mentioned|p341|||||||||
12822|Mount Isa Group|35892|6|Mentioned|p369|||||||||
12822|Mount Isa Group|35932|6|Mentioned|p461|||||||||
12822|Mount Isa Group|35950|6|Mentioned|p305|||||||||
12822|Mount Isa Group|36012|6|Mentioned|p16|||||||||
12822|Mount Isa Group|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|36548|6|Mentioned|p513|||||||||
12822|Mount Isa Group|36584|6|Mentioned|p367|||||||||
12822|Mount Isa Group|37217|6|Mentioned|p649|||||||||
12822|Mount Isa Group|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|37459|6|Mentioned|p423|||||||||
12822|Mount Isa Group|37462|4|Described|Table4.VII|||||||||
12822|Mount Isa Group|37464|6|Mentioned|p508|||||||||
12822|Mount Isa Group|37565|5|Briefly described|p2|||See also Fig.5||||||
12822|Mount Isa Group|37568|5|Briefly described|p84|||||||||
12822|Mount Isa Group|37569|6|Mentioned|p91|||||||||
12822|Mount Isa Group|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|37862|6|Mentioned|p587|||||||||
12822|Mount Isa Group|38156|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38232|6|Mentioned|p82|||||||||
12822|Mount Isa Group|38234|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|38235|6|Mentioned|p113|||||||||
12822|Mount Isa Group|38237|6|Mentioned|p132|||||||||
12822|Mount Isa Group|38276|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38278|6|Mentioned|Fig.1|||||||||
12822|Mount Isa Group|38345|6|Mentioned|p18|||||||||
12822|Mount Isa Group|38348|6|Mentioned|p6|||||||||
12822|Mount Isa Group|38350|4|Described|p15|||||||||
12822|Mount Isa Group|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Contains the Breakaway Shale, Moondarra Siltstone and the Warrina Park Quartzite.||||||25-AUG-04
12822|Mount Isa Group|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|38584|6|Mentioned|p17|||||||||
12822|Mount Isa Group|38598|6|Mentioned|p197|||||||||
12822|Mount Isa Group|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12822|Mount Isa Group|38833|6|Mentioned|p161|||||||||
12822|Mount Isa Group|38835|6|Mentioned|p164|||||||||
12822|Mount Isa Group|38836|6|Mentioned|p165|||||||||
12822|Mount Isa Group|38919|6|Mentioned|p493|||||||||
12822|Mount Isa Group|39043|6|Mentioned|p9|||||||||
12822|Mount Isa Group|39202|6|Mentioned|p242|||||||||
12822|Mount Isa Group|39362|6|Mentioned|p1468|||||||||
12822|Mount Isa Group|39445|4|Described|p41|||Shallow marine in parts-intermontane. See also p36, p40 and Table 2.||||||09-NOV-06
12822|Mount Isa Group|39492|6|Mentioned|p30|||||||||
12822|Mount Isa Group|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|39561|6|Mentioned|Fig.8|||||||||
12822|Mount Isa Group|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes: Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone.||||||15-JUN-06
12822|Mount Isa Group|39602|6|Mentioned|p603|||||||||
12822|Mount Isa Group|39622|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12822|Mount Isa Group|39934|6|Mentioned|p317|||See Fig.3||||||
12822|Mount Isa Group|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12822|Mount Isa Group|40105|6|Mentioned|p310|||||||||
12822|Mount Isa Group|40202|6|Mentioned|p719|||||||||
12822|Mount Isa Group|40221|4|Described|p19|||||||||
12822|Mount Isa Group|40394|6|Mentioned|Fig.2|||||||||
12822|Mount Isa Group|40598|6|Mentioned|p31|||||||||
12822|Mount Isa Group|40623|5|Briefly described|p95|||||||||
12822|Mount Isa Group|40788|6|Mentioned|p27|||||||||
12822|Mount Isa Group|40840|6|Mentioned|Map legend|||||||||
12822|Mount Isa Group|40984|5|Briefly described|p400|||||||||
12822|Mount Isa Group|41079|6|Mentioned|p296|||||||||
12822|Mount Isa Group|41248|5|Briefly described|p69|||||||||
12822|Mount Isa Group|41277|6|Mentioned|Fig.5|||||||||
12822|Mount Isa Group|41298|6|Mentioned|Map legend|Carpentarian||||||||
12822|Mount Isa Group|41307|5|Briefly described|p15|||||||||
12822|Mount Isa Group|41381|6|Mentioned|p323|||||||||
12822|Mount Isa Group|41466|6|Mentioned|p23|||||||||
12822|Mount Isa Group|41744|5|Briefly described|p407|||||||||
12822|Mount Isa Group|41791|6|Mentioned|p272|||||||||
12822|Mount Isa Group|41802|5|Briefly described|p530|||||||||
12822|Mount Isa Group|41975|6|Mentioned|p437|||||||||
12822|Mount Isa Group|41978|6|Mentioned|p502|||||||||
12822|Mount Isa Group|41979|6|Mentioned|Fig.2 P512|||||||||
12822|Mount Isa Group|42072|4|Described|p1615|||||||||
12822|Mount Isa Group|42234|6|Mentioned|Fig.2 P1055|||||||||
12822|Mount Isa Group|42323|6|Mentioned|p4|||||||||
12822|Mount Isa Group|42350|5|Briefly described|p542||Mesoproterozoic|See also Fig. 1 p543.||||||09-NOV-06
12822|Mount Isa Group|42365|5|Briefly described|p272|||||||||
12822|Mount Isa Group|42367|6|Mentioned|p18|||||||||
12822|Mount Isa Group|42503|5|Briefly described|p334|||||||||
12822|Mount Isa Group|42523|5|Briefly described|p372|||||||||
12822|Mount Isa Group|42565|5|Briefly described|Table 1 P5, P4|||||||||
12822|Mount Isa Group|42570|6|Mentioned|p548|||Actually spelt Mt. Isa Group.||||||
12822|Mount Isa Group|42766|6|Mentioned|p2|||||||||
12822|Mount Isa Group|42782|5|Briefly described|p458|||||||||
12822|Mount Isa Group|42818|5|Briefly described|p206, Fig.2 p205|||||||||
12822|Mount Isa Group|42819|5|Briefly described|p310|||||||||
12822|Mount Isa Group|43107|6|Mentioned|p8|||||||||
12822|Mount Isa Group|43486|5|Briefly described|21|||||||||
12822|Mount Isa Group|43583|6|Mentioned|p2164|||Age 1670+/-19 Ma||||||
12822|Mount Isa Group|43595|5|Briefly described|p353,441||Mesoproterozoic|Tuffs U-Pb zircon age:1670+/-19 Ma.||||||09-NOV-06
12822|Mount Isa Group|43608|6|Mentioned|Fig.11,p11|||||||||
12822|Mount Isa Group|43615|6|Mentioned|p13|||1653+/-7 Ma||||||
12822|Mount Isa Group|43616|6|Mentioned|p2|||||||||
12822|Mount Isa Group|43652|6|Mentioned|p388|||||||||
12822|Mount Isa Group|43664|6|Mentioned|p14|||||||||
12822|Mount Isa Group|43760|5|Briefly described|p431|||Tuff horizons dated at 1670 Ma.||||||09-NOV-06
12822|Mount Isa Group|43972|14|Not recorded|p7||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|44195|6|Mentioned|p350|||||||||
12822|Mount Isa Group|44389|14|Not recorded|p33||Paleoproterozoic|||||||07-NOV-08
12822|Mount Isa Group|44517|2|Defined|p234,237,239,map||Paleoproterozoic|Replaces Mount Isa Shale. Consists of Moondarra Silstone, Breakaway Shale, Native Bee Siltstone, Urquhardt Shale, Spear Siltstone, Kennedy Siltstone and Magazine Shale.||||||07-NOV-08
12822|Mount Isa Group|44755|14|Not recorded|Fig.1,p90,93||Mesoproterozoic|||||||
12822|Mount Isa Group|44764|4|Described|p33|||15,000' thick.||||||
12822|Mount Isa Group|44765|14|Not recorded|p15,16,18|||In Western Geosyncline.||||||
12822|Mount Isa Group|44766|14|Not recorded|unknown (23-27)|||Not listed on white card.||||||
12822|Mount Isa Group|44816|14|Not recorded|p20|||||||||
12822|Mount Isa Group|44827|14|Not recorded|p359|||||||||
12822|Mount Isa Group|45072|5|Briefly described|p5|||Sedimentation||||||
12822|Mount Isa Group|45136|4|Described|Table 1|||Also mention p19.||||||09-NOV-06
12822|Mount Isa Group|45161|5|Briefly described|p13|||See also p27.||||||09-NOV-06
12822|Mount Isa Group|45162|6|Mentioned|p45|||||||||
12822|Mount Isa Group|45166|4|Described|p28|||||||||
12822|Mount Isa Group|46801|6|Mentioned|p115|||See also Table 1||||||
12822|Mount Isa Group|46919|6|Mentioned|p221|||||||||
12822|Mount Isa Group|46960|6|Mentioned|p215|||||||||
12822|Mount Isa Group|46962|4|Described|Table 1|||See also Fig.3.||||||
12822|Mount Isa Group|46996|6|Mentioned|p273|||||||||
12822|Mount Isa Group|47011|6|Mentioned|p331|||||||||
12822|Mount Isa Group|47083|4|Described|p18-19|||Age: 1670 Ma. Correlates with McNamara Group. Overlies Surprise Creek Formation.  Mount Isa Orogen. Max thickness: 4250 m.||||||18-JAN-07
12822|Mount Isa Group|49041|5|Briefly described|Table 1|||||||||
12822|Mount Isa Group|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Age: ~1650Ma.||||||
12822|Mount Isa Group|50332|4|Described|p16, p50|Paleoproterozoic|Paleoproterozoic|Includes; Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale + Spear Siltstone. Age: ~1700-1640Ma. Geol Prov: Western Fold Belt Province. Fluvial and shallow marine/lacustrine sedimentary rocks and subordinate bimodal volcanics.||||||07-FEB-11
12822|Mount Isa Group|50536|6|Mentioned|p8.1|||Geological Province: Mount Isa Inlier.||||||
12822|Mount Isa Group|50550|6|Mentioned|p1141 Fig.4||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
12822|Mount Isa Group|50624|4|Described|p235||Statherian|Lists contained units. Unconformably overlies Haslingden Group. Thickness: 4000m.||||||
12822|Mount Isa Group|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Meta-arenite, quartzite, siltstone, shale.||||||
12822|Mount Isa Group|60558|5|Briefly described|p3, p4 Fig. 3, p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Includes seven units. Geological Province: Western Fold Belt.||||||03-JUN-09
12822|Mount Isa Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: western Mount Isa Block.||||||07-NOV-08
12822|Mount Isa Group|61732|6|Mentioned|p26|||||||||07-FEB-11
12822|Mount Isa Group|61735|5|Briefly described|p658|Paleoproterozoic|Paleoproterozoic|Age: ~1653Ma.||||||30-JUN-09
12822|Mount Isa Group|61736|5|Briefly described|p674|||Includes Native Bee Siltstone and Urquhart Shale.||||||
12822|Mount Isa Group|61922|5|Briefly described|p9 Fig. 3, p10|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. See also p19 Fig.11.||||||07-NOV-08
12822|Mount Isa Group|61923|5|Briefly described|p27, p28 Fig.1|||Includes the Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale and Native Bee Siltstone. Overlies Eastern Creek Volcanics. Geological Province: Mount Isa Inlier. Mount is Mt in text. See also p34 Fig.6.||||||
12822|Mount Isa Group|61924|6|Mentioned|p43 Fig.2B|||||||||
12822|Mount Isa Group|61933|6|Mentioned|p176|||Geological Province: Western Fold belt, Mount Isa Inlier.  Mount is Mt in text.||||||
12822|Mount Isa Group|61963|6|Mentioned|p776|||Hosts the Mount Isa Cu-Pb-Zn deposits.||||||23-MAR-06
12822|Mount Isa Group|62084|5|Briefly described|p936 Fig.5, p950 Fig.14|||Isa Superbasin. Mount Isa.|||Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear Siltstone, Kennedy Siltstone, Magazine Shale|||
12822|Mount Isa Group|62287|5|Briefly described|p130|Mesoproterozoic|Mesoproterozoic|Includes the Urquhart Shale.  Geological Province: Mount Isa Inlier.||||||09-NOV-06
12822|Mount Isa Group|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1655Ma.  Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
12822|Mount Isa Group|62535|5|Briefly described|p672, p674|Statherian|Statherian|Leichhardt River Fault Trough.|||Warrina Park Quartzite; Moondarra, Native Bee, Spear Siltstones; Breakaway, Urquhart, Magazine Shales; Kennedy Formation.||Includes dominant rhythmically laminated siliciclastic facies.|
12822|Mount Isa Group|62536|5|Briefly described|p658|||Mount Isa, Qld. Deposition and syngenetic mineralisation was followed 50-100 m.y. later by major deformational events.|1653 Ma (deposition).|||||
12822|Mount Isa Group|62873|5|Briefly described|p692|||Includes the Urquhart Shale in upper section. Sequence of carbonaceous and dolomitic siltstones, mudstones and shales. Overlies the Haslingden Group. Max. thickness: 6km.||||||22-NOV-06
12822|Mount Isa Group|63023|6|Mentioned|p1026|||Mount is Mt in text.||||||
12822|Mount Isa Group|63114|6|Mentioned|p1252. |||Isa superbasin.|||||Carbonate, carbonaceous siltstone, shale.|
12822|Mount Isa Group|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2, p294.  |Palaeoproterozoic|Palaeoproterozoic|Western Fold Belt. 4500 m thick.|ca 1670 Ma||||Dolomitic siltstone, shale.|
12822|Mount Isa Group|63866|6|Mentioned|p52|||||||||
12822|Mount Isa Group|63884|5|Briefly described|p14|||Metasedimentary rocks. Overlies Eastern Creek Volcanics. Mount is Mt in text.||||||
12822|Mount Isa Group|64137|6|Mentioned|p1544|||Mount Isa inlier. Same age as Tarcoola Formation.||||||
12822|Mount Isa Group|64250|5|Briefly described|p8, p25 fig 10, p11 fig.3, p19, p22, p24|||Detrital zircons age: 1730-1700 Ma probably from reworked material from NW. 1880-1850 Ma and ~ 1785 Ma are consistent with derivation from Murphy Inlier and Eastern Creek Volcanics.|1655 +/- 4 Ma||Breakaway, Urquhart, Magazine Shales; Moondarra, Native Bee, Spear-Kennedy Siltstones.||Mainly shales and siltstones.|
12822|Mount Isa Group|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Overlies Eastern Creek Volcanics. Max. thickness: 6km. Carbonaceous and dolomitic siltstones, mudstones and shales depositied in shallow water conditions.||||||07-FEB-11
12822|Mount Isa Group|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
12822|Mount Isa Group|64741|6|Mentioned|p310|||Temporal equivalents of upper parts of Willyama Supergroup.||||||07-FEB-11
12822|Mount Isa Group|64742|6|Mentioned|p334.|||||||||
12822|Mount Isa Group|64815|6|Mentioned|p3, |||||||||
12822|Mount Isa Group|65228|6|Mentioned|p9|||||||||
12822|Mount Isa Group|65337|6|Mentioned|p6.|||Isa Superbasin.||||||
12822|Mount Isa Group|65387|6|Mentioned|p85|||Widespread volcanism around 1690-1650 Ma is evident from tuff layers in this unit and the McNamara Group.||||||
12822|Mount Isa Group|65396|5|Briefly described|p16, p82, p173, p175, p188, p190, p193|Statherian|Statherian|See also p197, p241, p391, p439. Cover Sequence 3. Leichhardt River Fault Trough. Deposition mainly between c.1665 Ma and 1650 Ma. Hosts giant shale-hosted Pb-Zn-Ag+/-Cu deposits.|1655 +/- 4 Ma||Includes Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale, Spear-Kennedy Siltstone, Magazine Shale||Calcareous shales, pelites and mafic volcanics.|
12822|Mount Isa Group|66800|6|Mentioned|p928, p933.|||Western Fold Belt, Mount Isa Inlier. Hosts the Mount Isa and Hilton world-class, massive base-metal deposits.||||||
12822|Mount Isa Group|66824|6|Mentioned|p132, 135, 148-151|||Interpreted as a sag-phase sequence.||||Unconformably overlies Surprise Creek Formation. Equivalent to McNamara Group.|Includes laminated shales and dolomitic siltstones; tuff beds.|
12822|Mount Isa Group|66843|6|Mentioned|p35||||||includes Urquhart Shale.|||12-SEP-19
12822|Mount Isa Group|67026|4|Described|pp335-336.|Statherian|Statherian|4.5 - 6 km thick sequence of supracrustal volcanic and sedimentary rocks, deposited in a series of intracontinental extension-related basins.|1785 - 1650 Ma (Duncan et al. 2006).||Includes Urquhart Shale Formation.|Intruded by the Sybella Batholith c. 1660 Ma.|Sequence of carbonaceous and dolomitic siltstones, mudstones and shales.|24-APR-12
12822|Mount Isa Group|67323|4|Described|p8, p13, p15, p26, p34, p39, p72, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Isa Superbasin. Deposition began c.1670 Ma. Contains Ag anomalies.|~1675-1645 Ma.||Includes Breakaway Shale, Hero Formation, Kennedy Siltstone, Magazine Shale, Moondarra Siltstone, Native Bee Siltstone, Spear Siltstone, Urquhart Shale, Warrina Park Quartzite.|Unconformably overlies Oroopo Metabasalt.|Meta-arenite and quartzite, pyritic siltstone and shale; minor schist, micaceous metasiltstone|
12822|Mount Isa Group|67499|4|Described|p938-40, p941, p947, p948, p942 Fig.4|Statherian|Statherian|Equivalent to the McNamara Group - about 220km northwest of Mount Isa. Age estimated from p942 Fig.4.|1660 Ma||Includes Warrina Park Quartzite.|Stratigraphically equivalent to the McNamara Group.|Hosts important base-metal ores and consists of a basal silicified sandstone and conglomerate unit, overlain by several shale and siltstone units.|08-MAY-12
12822|Mount Isa Group|68020|6|Mentioned|p125, p126||||||Includes Urquhart Shale|Lower part correlated with Paradise Creek Formation.|Includes metasedimentary rocks.|
12822|Mount Isa Group|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|Western Succession.||||Overlies Surprise Creek Formation.||
12822|Mount Isa Group|68542|6|Mentioned|p6|||Cavaney (1975). Leichhardt River Fault Trough, Mount Isa Inlier.|||Includes Warrina Park Quartzite; Moondarra, Native Bee, Spear, Kennedy Siltstones; Breakaway, Urquhart, Magazine Shales.|Overlies Surprise Creek Beds.||
12822|Mount Isa Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
12822|Mount Isa Group|68576|5|Briefly described|Q_2: p6|||Cavaney (1975). Leichhardt River Fault Trough, Mount Isa Inlier.|||Warrina Park Quartzite; Moondarra, Native Bee, Spear, Kennedy Siltstones; Breakaway, Urquhart, Magazine Shales.|Overlies Surprise Creek Beds.||
12822|Mount Isa Group|68732|5|Briefly described|p159-163|||Mount spelt as Mt in text.|||Moondarra and Native Bee Siltstones, Urquhart Shale.||Includes cross-stratified quartzites and pebbly quartzites at or near the base.|01-DEC-17
12822|Mount Isa Group|69056|5|Briefly described|p54-56|||Isa Superbasin. Ore-bearing.|||Gun Supersequence.|Correlated with Tommy Creek Microgranite.||
12822|Mount Isa Group|69222|6|Mentioned|p221|Calymmian|Statherian|12-14km thick. Western Fold Belt; across the Lawn Hill Platform it is called the McNamara Group. Associated with the Mount Isa Rift Event. Age range c.1653-1595 Ma.|1652 +/- 7 Ma|||Overlies Surprise Creek Formation, Correlated with McNamara Group|Sag-related shale and dolomite rich sequences.|
12822|Mount Isa Group|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Surprise Creek Formation. Is intruded by Sybella Granite.||25-JAN-19
12822|Mount Isa Group|69542|5|Briefly described|p132, p133 Fig.2, p140|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.|||Includes Warrina Park Quartzite, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Urquhart Shale.||Laminated dolomitic and carbonaceous siltstone and shale.|
12822|Mount Isa Group|69591|4|Described|p29, p40, p42-45, p55, p108|Paleoproterozoic|Paleoproterozoic|Leichhardt River Domain, Isa Superbasin. Upper parts are mostly carbonaceous, and dolomitic argillites deposited in deeper water (deepwater rhythmites). Is coeval with 1653-1650 Ma Tommy Creek Microgranite.|~1660-1650 Ma (lower part).||Warrina Park Quartzite, Urquhart Shale, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone, Spear Siltstone, Kennedy Siltstone, Magazine Shale, Hero Formation.|Unconformably overlies Oroopo Metabasalt. Coeval with McNamara Group. Is faulted against Eastern Creek Volcanics and Myally Subgroup.|Dominated by carbonaceous and dolomitic siltstone and shale.|
12822|Mount Isa Group|70282|5|Briefly described|p544, p551|||Cover sequence 4, Mount Isa. Shallow-marine deposits.|> 1652 Ma||Urquhart Shale.|Overlies Surprise Creek Formation.|Siltstones and carbonate rocks.|13-FEB-18
12822|Mount Isa Group|70283|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Hosts the Mount Isa Cu and stratiform Pb-Zn-Ag deposits.|||Includes Surprise Creek Formation, Urquhart Shale|Overlies Haslingden Group|Metasediments: dolomitic siltstone, shale and carbonates, interbedded with minor tuff horizons, sulfates and minor halite evaporites.|14-FEB-18
12822|Mount Isa Group|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Warrina Park Quartzite; Moondarra, Native Bee Siltstones; Breakaway Shale.|||
12822|Mount Isa Group|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic||||Warrina Park Quartzite; Moondarra, Native Bee Siltstones; Breakaway Shale.|||
12822|Mount Isa Group|70897|5|Briefly described|p36||||c.1640 Ma.|||||
12822|Mount Isa Group|71606|5|Briefly described|p137|Statherian|Statherian|Leichardt River Fault Trough, Mount Isa Inlier.||||Underlain by Surprise Creek Formation. Equivalent to Fickling and McNamara groups.||
12822|Mount Isa Group|71960|5|Briefly described|p85-87, p77, p78, 81, 83, 104, 105|Proterozoic|Proterozoic|Originally defined by Bennet (1965). Redefined by Derrick et al. (1976) as comprising 8 formations. Four lowest in study area form a fining upwards megasequence (lower Mount Isa Group). Provenance of lower part shown to be from west. Also shows early deformation.|||Includes from base,  Warrina Park Quartzite, Hero Formation, Moondarra Siltstone, Breakaway Shale, Native Bee Siltstone.|Unconformably overlies/truncates Eastern Creek Volcanics in Hero Syncline, and other parts of the Haslingden Group elsewhere. Shown as equivalent to McNamara Group in Fig 8 p86.||
12822|Mount Isa Group|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Hero/Western Fault Zone.|||Includes Surprise Creek Formation, Warrina Park Quartzite, Hero Formation, Moondarra Siltstone, Breakaway Shale,|Unconformably overlies Haslingden Group.||03-APR-19
12822|Mount Isa Group|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.|||Magazine Shale, Spear-Kennedy Siltstone, Urquhart Shale, Native Bee Siltstone, Breakaway Shale and Moondarra Siltstone.|Shown as unconformably and partially overlying Torpedo Creek and Warrina Park Quartzites.|Includes shale and siltstone.|
12822|Mount Isa Group|72889|6|Mentioned|p6 Fig.i.|||||||||
12822|Mount Isa Group|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian||||Magazine, Urquhart and Breakaway Shale, Spear-Kennedy, Native Bee and Moondarra Siltstone.|Shown as unconformably overlying Torpedo Creek and Warrina Park Quartzite. Laterally and partially equivalent to McNamara Group.|Includes carbonaceous and dolomitic siltstones andshales.","Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Isa Superbasin, Mount Isa Province.|
12822|Mount Isa Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Isa Superbasin.|||Magazine Shale, Spear-Kennedy Siltstone, Urquhart Shale, Native Bee Siltstone, Breakaway Shale, Moondarra Siltstone.|||
12822|Mount Isa Group|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
12822|Mount Isa Group|73413|6|Mentioned|p3|||Mount Isa Inlier.||||||
12828|Mount Isa Tuff Marker Bed|37217|6|Mentioned|Table 1|||||||||
12856|Mount Joy Basalt|23619|4|Described|p28 table 1|||Of the McBride Basalt Group in the McBride Basalt Province.||||||
12856|Mount Joy Basalt|41680|6|Mentioned|p106|||||||||
12856|Mount Joy Basalt|43113|4|Described|Table 1 p16||Pleistocene|of McBride Basalt Group.||||||
12856|Mount Joy Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
12856|Mount Joy Basalt|50201|5|Briefly described|Map Legend|Quaternary|Quaternary|Of the McBride Basalt Group.||||||
12856|Mount Joy Basalt|50202|5|Briefly described|Map legend|Quaternary|Quaternary|Of the McBride Basalt Group.  Olivine basalt.  Age <0.4Ma.||||||
12856|Mount Joy Basalt|60360|5|Briefly described|Map Legend|Quaternary|Quaternary|Of the McBride Basalt Group. Olivine basalt. Age: <0.4Ma.||||||20-JUN-13
12856|Mount Joy Basalt|68344|5|Briefly described|Map legend.|Quaternary|Quaternary||<0.4 Ma.|Unit in McBride Basalt Group.|||Olivine basalt.|
12856|Mount Joy Basalt|68346|5|Briefly described|Map legend.|Quaternary|Quaternary|Of McBride Basalt Province.|<0.4 Ma.|Unit in McBride Basalt Group.|||Olivine basalt.|
12856|Mount Joy Basalt|68477|5|Briefly described|Map Legend|Pleistocene|Pleistocene|McBride Basalt Province.|< 0.4 Ma|Of the McBride Basalt Group.|||Olivine Basalt.|
12856|Mount Joy Basalt|68576|5|Briefly described|Q_11: p20 Fig.17|Pleistocene|Pliocene|McBride Basalt Province, Einasleigh-Mount Surprise area.||||||
12856|Mount Joy Basalt|73115|6|Mentioned|p28-29, p39, p43, p48, p53, p59, p65|Pleistocene|Pleistocene|McBride Basalt Province.|0.4 Ma|||||
12859|Mount Jukes Intrusive Complex|23042|4|Described|p104, Fig 2||Tertiary|Intrudes Calen Coal Measures.||||||
12859|Mount Jukes Intrusive Complex|40577|6|Mentioned|p49|||||||||
12859|Mount Jukes Intrusive Complex|60787|5|Briefly described|p9|Tertiary|Tertiary|||||||13-JUN-05
12859|Mount Jukes Intrusive Complex|65388|3|Fully described|p420-422, 426|Oligocene|Eocene|Includes Blackwood Quartz Syenite, Neilson Leucogabbro, Jukes Granite and Seaforth Microgranite. Previously called Mount Jukes Syenite Complex. Intrudes Calen Coal Measures and Carmila beds.||||||
12859|Mount Jukes Intrusive Complex|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as the Silver Plains Nephelinite, Tabor Gabbro, Mount Barney Central Complex, and unnamed basaltic to rhyolitic plugs, are all mapped under the symbol, Ti.||||||
12859|Mount Jukes Intrusive Complex|68679|5|Briefly described|p347|Paleogene|Paleogene|Northern New England Orogen.||||||
12859|Mount Jukes Intrusive Complex|69599|5|Briefly described|p634|||Clarke et al. (1971) and others. Cape Hillsborough. A 7 x 3 km oval complex of stocks.|34.1 +/- 0.9 Ma to 31.1 +/- 0.8 Ma.||Neilson Leucogabbro, Jkkes Granite, Blackwood Quartz Syenite, Seaforth Microgranite.|||
12859|Mount Jukes Intrusive Complex|73450|5|Briefly described|p4, p45, p71-73|||Exposed syenitic to gabbroic intrusions interpreted to represent shallow plumbing systems. [Also written as Jukes Intrusive Complex in Fig.II, p4].|||Neilson Leucogabbro, Blackwood Quartz Syenite, Jukes Granite, Seaforth Microgranite||Includes syenitic to gabbroic intrusions.|
12870|Mount Killabakh comendite|40586|6|Mentioned|p408|||||||||
12881|Mount Lawless complex|40479|6|Mentioned|p33|||||||||
12881|Mount Lawless complex|40954|6|Mentioned|p133|||||||||
12886|Mount Les Siltstone|22453|6|Mentioned|p 12|||In the McArthur Basin.||||||09-NOV-06
12886|Mount Les Siltstone|22665|5|Briefly described|Table1, P229||Statherian|Mount actually spelt Mt, Age of unit is 1640+/-7 Ma.||||||09-NOV-06
12886|Mount Les Siltstone|22673|3|Fully described|63-66, 76,78|||Geological province: Mount Isa Basin. Mount as 'Mt' in text.||||||09-NOV-06
12886|Mount Les Siltstone|22680|6|Mentioned|83,85,87|||Geological province: Mount Isa Basin. Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|23031|6|Mentioned|27|||Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|23065|6|Mentioned|16|||Of the Fickling Group. Age 1640 +/- 7 Ma||||||09-NOV-06
12886|Mount Les Siltstone|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
12886|Mount Les Siltstone|23396|4|Described|p417|Statherian|Statherian|Of Fickling Group. Age: 1640+/-7Ma.||||||28-SEP-06
12886|Mount Les Siltstone|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1640+/-7Ma.||||||09-NOV-06
12886|Mount Les Siltstone|23398|4|Described|p445|Statherian|Statherian|Age: 1640+/-7Ma.||||||28-SEP-06
12886|Mount Les Siltstone|23406|5|Briefly described|p606, p608 Fig. 9, p613|Statherian|Statherian|Of Fickling Group. Age: 1640+/-7Ma. Consists of interbedded, fine-grained sandstone, siltstone and shale with occasional thin dolostone beds.||||||16-JUN-09
12886|Mount Les Siltstone|23409|5|Briefly described|p533|||Of the Fickling Group.||||||09-NOV-06
12886|Mount Les Siltstone|24308|5|Briefly described|p1002, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Mount is Mt. in text.  Of the Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
12886|Mount Les Siltstone|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Age: 1640+/-7 Ma. Carbonaceous, dolomitic and pyritic shales and local talus breccias. Overlies Walford Dolomite. Geological Province: Lawn Hill Platform.||||||25-FEB-05
12886|Mount Les Siltstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|36012|3|Fully described|Table 3|||See also p16.||||||28-SEP-06
12886|Mount Les Siltstone|36217|6|Mentioned|p206|||Published by Grimes & others 1979. Definition approved by Qld SNC.||||||
12886|Mount Les Siltstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|38237|6|Mentioned|p129|||||||||
12886|Mount Les Siltstone|38348|6|Mentioned|p13|||||||||
12886|Mount Les Siltstone|38584|4|Described|p17|||||||||
12886|Mount Les Siltstone|39445|5|Briefly described|Table 2|||See also p39.||||||09-NOV-06
12886|Mount Les Siltstone|39497|6|Mentioned|Fig.4|||||||||
12886|Mount Les Siltstone|39685|6|Mentioned|p407|||||||||
12886|Mount Les Siltstone|39925|6|Mentioned|Fig.9|||||||||
12886|Mount Les Siltstone|41721|4|Described|p28|||||||||
12886|Mount Les Siltstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
12886|Mount Les Siltstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Fickling Group. Of "Mid Proterozoic" age.||||||09-NOV-06
12886|Mount Les Siltstone|45162|6|Mentioned|p146|||||||||
12886|Mount Les Siltstone|45166|5|Briefly described|p30|||||||||
12886|Mount Les Siltstone|49001|2|Defined|p10|Carpentarian|Carpentarian|||||||
12886|Mount Les Siltstone|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Overlian by Doomadgee Formation, underlain by Walford Dolomite.||||||
12886|Mount Les Siltstone|61936|5|Briefly described|p194 Fig. 6|||Age: <1640Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||15-MAR-07
12886|Mount Les Siltstone|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform.|1640 +/- 7 Ma.|McNamara Group.||||
12886|Mount Les Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Mount is Mt in text. Overlain by Riversleigh Siltstone. Geological Province: Isa Superbasin. Consists of siltstone and shale.||||||30-SEP-08
12886|Mount Les Siltstone|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of River Supersequence. Age: 1644+/-8 and 1640+/-7Ma. Geological Province: Isa Superbasin. Consists of conglomerates and fine-grained arenites.||||||07-FEB-11
12886|Mount Les Siltstone|63113|6|Mentioned|p1225 Fig.13, p1226. |||Isa Superbasin. River supersequence. The probable source of hydrocarbons deposited in Walford Dolomite.||||Overlies Walford Dolomite.||
12886|Mount Les Siltstone|63115|6|Mentioned|1279 Fig.4,p1281, |||Isa superbasin. Hosts the Walford Creek Cu-Zn-Pb-bearing stratiform pyrite lenses.||Unit in Fickling Group.|||Includes metalliferous dolomitic black shales.|
12886|Mount Les Siltstone|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
12886|Mount Les Siltstone|63866|5|Briefly described|p56|Statherian|Statherian|Isa Superbasin.|1640 +/- 7 Ma|||Equivalent to the River Supersequence.||
12886|Mount Les Siltstone|65228|5|Briefly described|p33, Fig.04.|Statherian|Statherian|Mt Les in text. Only component of River Supersequence at the northern end of Lawn Hill Platform.|1640 +/- 7 Ma (SHRIMP).|||||
12886|Mount Les Siltstone|65337|6|Mentioned|p22 Table 4.|||||Unit in Fickling Group.||Is overlain by Doomadgee Formation.||
12886|Mount Les Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin.|1640 +/- 7 Ma (maximum depositional age).|Fickling Group.|||Dolomitic siltstone and shale; flaggy dolomite interbeds|
12886|Mount Les Siltstone|68733|5|Briefly described|p186|Statherian|Statherian|||Of the McArthur Group.||||
12886|Mount Les Siltstone|69433|4|Described|p18:2-4|Statherian|Statherian|Northern succession, Lawn Hill Platform. Up to 90m thick. Evaporitic conditions in a supratidal environment. SHRIMP U-Pb zircon age from a tuffaceous bed, by Page and Sweet (1998), Page et al. (2000). Misspelt as Mount Less Siltstone in table 18.1, p18:4.|1640 +/- 7 Ma.|Fickling Group.||Conformably overlies Walford Dolostone. Is overlain disconformably by Doomadgee Formation.|Dolostone, siltstone, shale and minor interbeds of flaggy dolostone with gypsum and pyrite pseudomorphs.|23-APR-20
12886|Mount Les Siltstone|69591|4|Described|p43 Fig.2.31, p47|||Camooweal-Murphy Domain, Isa Superbasin. S of the Murphy Inlier. Part of the River Supersequence. Deep marine deposits.|1640 +/- 7 Ma (Page and Sweet, 1998).|Fickling Group.||Equivalent of the Riversleigh Siltstone.|Dolomitic siltstone and shale; flaggy dolomite interbeds.|
12886|Mount Les Siltstone|69673|4|Described|p52 fig 42, p53 , p54 |Statherian|Statherian||1640 +/- 7 Ma||||Dolostone, siltstone, shale and minor interbeds of flaggy dolostone with gypsum and pyrite pseudomorphs.|
12886|Mount Les Siltstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Overlies Walford Dolostone. Is overlain unconformably by Doomadgee Formation.|Dolomitic siltstone and shale; flaggy dolomite interbeds.|
12886|Mount Les Siltstone|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1641+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
12886|Mount Les Siltstone|72526|5|Briefly described|p8 Fig.1.3, p20.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1640 +/-7 Ma|Fickling Group||Overlies Walford Dolomite and disconformably underlies Doomadgee Formation.||
12886|Mount Les Siltstone|72912|5|Briefly described|p5 Fig.3, p32, p33 Fig.12, p45.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. U-Pb zircon sedimentary depositional age given.|1640 +/- 7 Ma|Fickling Group||Overlies Walford Dolomite and unconformably underlies Doomadgee Formation. Partially equivalent to Lawn Hill Formation and Shady Bore Quartzite. Laterally equivalent to Plain Creek Formation.|Includes organic rich siltstone and shales.|
12886|Mount Les Siltstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p22, p24, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin.  Identified in 3 wells in this study. Mineral composition shows majority quartz, microcline, muscovite and dolomite.|1640 +/- 7 Ma|Fickling Group||Overlies Walford Dolomite and unconformably underlies Doomadgee Formation.|Includes siltstone.|
12886|Mount Les Siltstone|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||Fickling Group||||
12886|Mount Les Siltstone|73042|5|Briefly described|p1, p4, p6, p14, p17|Statherian|Statherian|Previous zircon U-Pb age data on a tuff interval yielded a depositional age of 1640+/-7 Ma (Page and Sweet, 1998). Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Maximum thickness: <100m. Parent unit is said to be the Fickling Group throughout; however, is indicated as the McNamara Group on p18 (wrong parent?).|1640 +/- 7 Ma|Fickling Group||Conformably underlain by Walford Dolomite. Disconformably overlain by Doomadgee Formation.|Dolostone, siltstone and shale with minor occurrences of flaggy dolostone with gypsum and pyrite pseudomorphs.|
12888|Mount Leyshon Complex|23988|5|Briefly described|p19 Fig.10|||Mount is Mt. in text.||||||
12888|Mount Leyshon Complex|24334|5|Briefly described|p54 Tb.2|Early Permian|Early Permian|Age: 286 Ma. Mount is Mt in text.||||||
12888|Mount Leyshon Complex|41806|6|Mentioned|Fig.2|||||||||
12888|Mount Leyshon Complex|43934|5|Briefly described|Map Legend||Carboniferous|||||||
12888|Mount Leyshon Complex|50153|5|Briefly described|p4|Carboniferous|Carboniferous|Of Ravenswood Arch (Lolworth Ravenswood Block). High level intrusive complex associated with porphyries, rhyolitic lavas and pyroclastics||||||
12888|Mount Leyshon Complex|67028|6|Mentioned|p371 Tb. 5|Permian|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|280-292 Ma magnetic age range|||||10-AUG-15
12910|Mount Marcella Volcanics|22846|6|Mentioned|p63||Middle Triassic|Intruded by Boonara Granodiorite.||||||
12910|Mount Marcella Volcanics|23799|6|Mentioned|p42|||Equivalent of Neara Volcanics (Esk Trough).||||||
12910|Mount Marcella Volcanics|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|Parent: Toogoolawah Group.||||||14-AUG-08
12910|Mount Marcella Volcanics|41738|2|Defined|p166|Middle Triassic||||||||
12910|Mount Marcella Volcanics|41778|6|Mentioned|Table 2|||||||||
12910|Mount Marcella Volcanics|41790|5|Briefly described|p474|||||||||
12910|Mount Marcella Volcanics|42054|6|Mentioned|p272|||||||||
12910|Mount Marcella Volcanics|42902|5|Briefly described|p416|||Actually spelt Mt Marcella Volcanics.||||||14-AUG-08
12910|Mount Marcella Volcanics|61782|6|Mentioned|p275|||Mount is 'Mt' in text. Of Toogoolawah Group. Geol Prov: Esk Trough.||||||
12910|Mount Marcella Volcanics|61809|6|Mentioned|p457|Triassic|Triassic|Overlies Gympie Group. Geological Province: New England Orogen.||||||
12910|Mount Marcella Volcanics|63821|5|Briefly described|p20|Late Triassic|Middle Traissic|Of Toogoolwah Gp. Over Gayndah Fm. Intruded by Degilbo Granite. Age: 236ma, 237Ma (K-Ar). Geol.Prov: Esk Trough. Greenish, high-K andesitic volcanic+oligomictic volcaniclastics, conglom., sandst., minor polymictic conglom., pyroclastics+minor mudstone.||||||07-FEB-11
12910|Mount Marcella Volcanics|65452|5|Briefly described|p7 Tb.2, p37|Late Triassic|Middle Triassic|Gayndah area. SHRIMP U-Pb zircon magmatic crystallisation age (few zircons).|230.7 +/- 3.2 Ma (Cross, in prep.).||||Pyroxene andesite.|
12910|Mount Marcella Volcanics|67203|4|Described|p1, p3-4, p35-37|Late Triassic|Middle Triassic|One of several coeval stratovolcanoes in central to southeast Queensland. Mafic to intermediate lavas are geochemically similar to those in Bobby Volcanics and Agnes Waters Volcanics: may have formed in one continuous >100km long volcanic field. Unpublished ages from Cross, replacing the previous belief that this unit was early Middle Triassic.|230.7 +/- 3.2 Ma and 228.5 +/- 2.8 Ma.|||Is correlated with Bobby and Agnes Water Volcanics. Equivalent to Neara Volcanics.|Lower part is widespread and comprises basaltic to andesitic lavas interspersed with dacitic pyroclastics and fluvial volcaniclastics; includes pyroxene andesite and dacite ignimbrite.|
12910|Mount Marcella Volcanics|67874|5|Briefly described|p2-3, p8, p10-13, p17-20, p34, p49|Late Triassic|Middle Triassic|Northern Esk Trough. Mafic to intermediate-dominated. Developed in two stages: the Penwhaupell Volcanic Centre, followed after a period of sedimentation by the Ettiewyn Caldera. SHRIMP U-Pb zircon magmatic crystallisation age.|228.2 +/- 2.8 Ma (Cross et al., 2012).|Toogoolawah Group.||Equivalent to Neara Volcanics.|Interbedded lavas and pyroclastic deposits dominated by dacite, under caldera-formation andesite and andesitic ignimbrite.|
12910|Mount Marcella Volcanics|68679|5|Briefly described|p391, p434, p436-441|Late Triassic|Middle Triassic|Cranfield (1989). Gayndah region, northern Esk Basin. Development of the unit described in detail. Previously considered correlative of Neara Volcanics; disproved by Middle or Late Triassic plant fossils and isotope dating. Hosts porphyry Cu-Mo-Au deposits (e.g. Booubyjan).|228.5 +/- 2.8 Ma (SHRIMP: Cross et al., 2012).|||Is overlain unconformably by the Woodmillar Andesite (Aranbanga Volcanic Group). Older parts are equivalent to (a northern extension of) the Neara Volcanics.|A lower succession of interbedded basaltic-andesite (rare) to high silica dacite (dominant) lavas and pyroclastic deposits and an upper succession of andesitic lavas and pyroclastic deposits; separated by ?10 m.y. of sedimentation.|
12910|Mount Marcella Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|231 Ma (crystallisation: U-Pb zircon SHRIMP)||||Andesite, ignimbrite.|
12910|Mount Marcella Volcanics|73197|6|Mentioned|p481-482|Late Triassic|Late Triassic|New England Orogen, northern. Northern end of the Esk Basin.|ca 230 U-Pb zircon||||Dacitic to andesitic volcanics.|
12910|Mount Marcella Volcanics|73450|6|Mentioned|p24, p29, p32, p35|late Triassic|late Triassic|[Also written as Marcella Volcanics, p29]. Calc-alkaline continental arc magmatism. Volcanic rocks are truncated by Mount Walsh Granite.||||Overlain by Aranbanga Volcanic Group. Intruded by Hogback Granite, Mungore Granite and Mount Walsh Granite.||
12931|Mount Mee Granophyre|24418|5|Briefly described|p5, Map1|Late Triassic|Late Triassic|North west-trending dyke 11km long and up to 1km wide. varies from normal granophyre in the south to spherulitic granophyre at the northern end. May have been feeder to the Mount Byron Volcanics. Mount is Mt in geology map legend.||||||
12931|Mount Mee Granophyre|33902|6|Mentioned|p128|||Permian. Map.||||||
12931|Mount Mee Granophyre|36440|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
12931|Mount Mee Granophyre|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
12931|Mount Mee Granophyre|39079|6|Mentioned|p8|||||||||
12931|Mount Mee Granophyre|44783|14|Not recorded|p32|||||||||
12931|Mount Mee Granophyre|68679|5|Briefly described|p427, p436|Late Triassic|Late Triassic|Esk area. A narrow, elongate, NW-trending unit. Mat be comagmatic with the Mount Byron Volcanics.||||Intrudes Mount Byron Volcanics.|Granophyric dyke-like unit.|
12978|Mount Norna Quartzite|22460|5|Briefly described|p446|||Spelt 'Mt" in text. Also see Fig 1 p446. Of the Soldiers Cap Group.||||||18-JAN-07
12978|Mount Norna Quartzite|22461|5|Briefly described|Fig 1 p464|||||||||
12978|Mount Norna Quartzite|22467|4|Described|Fig 2 p431.|||Also see p432.||||||
12978|Mount Norna Quartzite|22483|5|Briefly described|p418.|||Of the Maronan Supergroup.||||||18-JAN-07
12978|Mount Norna Quartzite|22513|6|Mentioned|p.373|||||||||
12978|Mount Norna Quartzite|22523|5|Briefly described|p364-365,Fig15p371|||||||||
12978|Mount Norna Quartzite|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with Etheridge Group (Qld) Corbet Formation.||||||07-NOV-08
12978|Mount Norna Quartzite|23067|6|Mentioned|p794|||||||||
12978|Mount Norna Quartzite|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1654+/-4Ma.||||||18-JAN-07
12978|Mount Norna Quartzite|23613|5|Briefly described|p725|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group.||||||07-NOV-08
12978|Mount Norna Quartzite|23962|5|Briefly described|p1215 Fig. 2|||Geological Province: Mount Isa Inlier.  Of the Soldiers Cap Group.||||||16-DEC-04
12978|Mount Norna Quartzite|24039|6|Mentioned|p463|Paleoproterozoic|Paleoproterozoic|Mount is Mt. in text.||||||07-NOV-08
12978|Mount Norna Quartzite|24254|5|Briefly described|p19 Fig.2|||Geological Province: Eastern Fold Belt, Mount Isa Inlier. Of the Soldiers Cap Group.||||||18-JAN-07
12978|Mount Norna Quartzite|24259|6|Mentioned|p114|||||||||
12978|Mount Norna Quartzite|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of Soldiers Cap Group. Overlies Llewellyn Creek Formation. Overlain by Toole Creek Volcanics. Age: 1654+/-4 Ma. Geological Province: Eastern Fold Belt.||||||
12978|Mount Norna Quartzite|24462|5|Briefly described|p297||Paleoproterozoic|Of the Soldiers Cap Group.  Mount is Mt. in text.  Age: 1693Ma and 1654+/-4Ma.  Geological Province: Mount Isa Block.||||||07-NOV-08
12978|Mount Norna Quartzite|33900|6|Mentioned|p17|||||||||
12978|Mount Norna Quartzite|35074|6|Mentioned|Fig.2|||||||||
12978|Mount Norna Quartzite|35295|2|Defined|p601|Precambrian|Precambrian|||||||
12978|Mount Norna Quartzite|35388|6|Mentioned|Fig.10|||||||||
12978|Mount Norna Quartzite|37568|5|Briefly described|p81|||||||||
12978|Mount Norna Quartzite|37569|6|Mentioned|p90|||Originally recorded as in NT. Corrected 18-MAR-92.||||||
12978|Mount Norna Quartzite|38276|6|Mentioned|Fig.1|||||||||
12978|Mount Norna Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12978|Mount Norna Quartzite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
12978|Mount Norna Quartzite|39445|5|Briefly described|Table 2|||See also p42.||||||18-JAN-07
12978|Mount Norna Quartzite|39496|5|Briefly described|p7|||||||||
12978|Mount Norna Quartzite|39622|6|Mentioned|p26|||See also Fig.2||||||
12978|Mount Norna Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
12978|Mount Norna Quartzite|40840|6|Mentioned|Map legend|||||||||
12978|Mount Norna Quartzite|41272|6|Mentioned|M 1of1 C07|||||||||
12978|Mount Norna Quartzite|41464|6|Mentioned|Map legend|Proterozoic||||||||
12978|Mount Norna Quartzite|41556|6|Mentioned|Map legend|Proterozoic||||||||
12978|Mount Norna Quartzite|41568|3|Fully described|p7|||||||||
12978|Mount Norna Quartzite|41791|5|Briefly described|p263|||Originally recorded as in NT. Corrected 18-MAR-92.||||||
12978|Mount Norna Quartzite|41978|3|Fully described|Table 1 P492|||||||||
12978|Mount Norna Quartzite|43614|6|Mentioned|p19|||||||||
12978|Mount Norna Quartzite|43616|6|Mentioned|p4|||||||||
12978|Mount Norna Quartzite|43618|6|Mentioned|p41|||||||||
12978|Mount Norna Quartzite|43767|6|Mentioned|p894|||||||||
12978|Mount Norna Quartzite|44195|5|Briefly described|p345 Table 1,350|||U-Pb ion probe ages given: Maximum depositional age: 1693 +/-5 Ma, age of rhyolite crystallisation in upper part of unit: 1654+/-4Ma||||||22-JUL-13
12978|Mount Norna Quartzite|45161|5|Briefly described|Table 12|||||||||
12978|Mount Norna Quartzite|45166|5|Briefly described|p25|||Entered as NT unit. Corrected 4-Mar-92.||||||
12978|Mount Norna Quartzite|46801|5|Briefly described|Fig.14, p124|Proterozoic|Proterozoic|Name for Weatherly Creek Quartzite.||||||
12978|Mount Norna Quartzite|49041|6|Mentioned|p6|||||||||
12978|Mount Norna Quartzite|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Of the Soldiers Cap Group. Fine-grained quartzite, metagreywacke, siltstone, chert, limestone, BIF, tuff, amphibolite and metabasalt. Overlies the Llewellyn Creek Formation.  See also p46, p73.||||||
12978|Mount Norna Quartzite|50125|4|Described|p87, p89|||Of the Soldiers Cap Group. Maximum Thickness: 2700m. Conformably overlies the Llewellyn Creek Formation. Conformably overlain by the Toole Creek Volcanics. Mount is Mt in text. Geological Province: Mount Isa Inlier.||||||
12978|Mount Norna Quartzite|50332|4|Described|p16, p21, p61 Fig. 17, p67|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group. Underlain by Llewellyn Creek Formation.  Age: 1695-1600Ma. Geol Prov: Cloncurry Subprovince. Consists of fine-grained quartzite, metagreywacke, siltstone, chert, limestone, banded iron formation, tuff, amphibolite + metabasalt.||||||07-FEB-11
12978|Mount Norna Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Soldiers Cap Group. Meta-arenite, mica schist, phyllite, amphibolite.||||||
12978|Mount Norna Quartzite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1650Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
12978|Mount Norna Quartzite|61922|5|Briefly described|p9 Fig. 3, p10|Paleoproterozoic|Paleoproterozoic|Of Soldiers Cap Group. Interbedded psammites/pelites, muscovite schist.  Age: 1654+/-4Ma. Overlies Llewellyn Creek Fm; overlain by Toole Creek Volcanics. Max. thickness: 2km. Geol. Prov: Mount Isa Inlier/Eastern Fold Belt.||||||07-NOV-08
12978|Mount Norna Quartzite|61925|5|Briefly described|p56 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1654+/-4Ma near top of unit. Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||07-NOV-08
12978|Mount Norna Quartzite|61926|5|Briefly described|p71 Fig. 1, p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||07-NOV-08
12978|Mount Norna Quartzite|61927|5|Briefly described|p95|||Metasedimentary unit. Mount is Mt in text.||||||
12978|Mount Norna Quartzite|61929|5|Briefly described|p127, p129 Fig. 3|||Of the upper part of Soldiers Cap Group. Feldspathic psammite, thin pelite, minor calc-silicate; thin BIFs. Age: max. of 1658Ma. Geological Province: Calvert Superbasin.||||||
12978|Mount Norna Quartzite|61936|5|Briefly described|p190 Fig. 3|||Includes turbidites. Geological Province: Eastern Fold Belt, Mount Isa Inlier. Mount is Mt in text.  See also p195 Fig. 6.||||||
12978|Mount Norna Quartzite|62047|6|Mentioned|p91 Fig.2 |||||||||
12978|Mount Norna Quartzite|63866|5|Briefly described|p63-p64|Statherian|Statherian|Records a range in metamorphic grade from amphibolite facies to granulite facies.|c. 1685 Ma|Soldiers Cap Group||||
12978|Mount Norna Quartzite|64248|6|Mentioned|p38 Fig.5|Statherian|Statherian||1654 +/- 4 Ma.|Soldiers Cap Group||||
12978|Mount Norna Quartzite|64249|5|Briefly described|p84 Fig. 2, p85, p86, p87, p89, p101-102|||Age: 1654Ma. Geological Province: Mount Isa Inlier.||||||21-APR-09
12978|Mount Norna Quartzite|64250|5|Briefly described|p10, p11 fig 3, p12, p14, p20|||Common detrital zircons dates: 1750-1730 Ma however they may not all correlate with this unit. Part of continuous depositing sequence with Llewellyn Creek Formation and Toole Creek Volcanics.|1654 +/- 4 Ma|Soldiers Cap Group||Possibly overlies Gandry Dam Gneiss, Kuridala Formation, Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics. Possibly correlates with Staveley Formation or Marimo Slate.|Quartzite, feldspathic quartzite, schist; minor metabasalt, conglomerate, felsic volcanics, BIF and marble.|
12978|Mount Norna Quartzite|64252|5|Briefly described|p70 Fig. 1, p71, p77|||Of Soldiers Cap Group. Geological Province: Mount Isa Inlier. Quartzites.||||||
12978|Mount Norna Quartzite|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
12978|Mount Norna Quartzite|65396|4|Described|p7, p12, p16-17, p82, p84, p90, p101-102|Statherian|Statherian|See also p105, p124, p134, p161, p169, p175-178, p183-184, p188-190, p195, p197-198, p202, p241, p344, p440. Isa Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. Metamorphic reaction detailed. Has similarities with Staveley Formation. Detrital zircon sources listed.|1654 +/- 4 Ma (Page and Sun, 1998), 1693 +/- 5 Ma|Soldiers Cap Group||Conformably overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics.|Quartzite, feldspathic quartzite and schist. Minor marble, banded iron formation, metabasalt, conglomerate and felsic metavolcanics.|04-APR-17
12978|Mount Norna Quartzite|65755|6|Mentioned|p2|||Part of Soldiers Cap Group in the north, Cloncurry Fault Zone. Written Mt in text.||||||
12978|Mount Norna Quartzite|65887|4|Described|p51|Statherian||Of Soldiers Cap Group. Conformably overlies Llewellyn Creek Formation. Conformably overlain by Toole Creek Volcanics. Quartzite, psammo-pelite, pelite and intercalated metadolerite sills and lesser metabasalt. Aged 1654+/-4 Ma (Page and Sun, 1998).||||||
12978|Mount Norna Quartzite|66913|5|Briefly described|p170 fig 1, p172|||Mineralisation?1690-1650 Ma.|Deposition 1710-1670 Ma.|Of Soldiers Cap Group.|||Includes turbidites, quartzite, basalt, and dolerite.|
12978|Mount Norna Quartzite|67323|4|Described|GIS attrib tbl, p19, p21, p26, p35, p57|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin. Turbidite deposits on a continental slope. Characterised by bluish quartzite.|~1685 Ma (MDA: Neumann et al., 2009).|Soldiers Cap Group.||Correlated with New Hope Quartzite.|Fine-grained quartz sandstone, siltstone and mudstone; minor chert, limestone; grades into quartzite and schist|
12978|Mount Norna Quartzite|67498|6|Mentioned|p920 Fig.2, p927-929, Fig.8, p932 Fig.10|||See also references to the informally-named Mount Norna Formation (p919, 924, 925, Fig.4, Fig.8, Fig.11).||Of the Soldiers Cap Group.|||Fine-grained quartzite, metamorphosed greywacke, siltstone, chert, limestone.|08-MAY-12
12978|Mount Norna Quartzite|67539|4|Described|p13|Statherian|Statherian|Middle unit. Detrital zircon age.|c. 1680 - 1670 Ma|Of the Soldiers Cap Group.||Equivalent of the New Hope Sandstone. Underlain by the Llewellyn Creek Volcanics? Overlain by the Toole Creek Volcanics?||
12978|Mount Norna Quartzite|68146|5|Briefly described|p201|||Suggested (Neumann, 2007) to be a lateral equivalent of the Kuridala Formation. Asge determination by Neumann et al. (2009).|1688 +/- 6 Ma maximum depositional age.|Soldiers Cap Group.||Overlies Llewellyn Creek Formation.||
12978|Mount Norna Quartzite|68542|6|Mentioned|p16 fig 4|||||||||
12978|Mount Norna Quartzite|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 3 (1690-1650 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
12978|Mount Norna Quartzite|68732|5|Briefly described|p163, p164, p165 Fig.3|Statherian|Statherian|Detrital zircon maximum sedimentary depositional ages.|1685 +/- 5, 1686 +/- 7 Ma||||Sandstones grading up into laminated siltstones and shales; packages several kilometres thick.|01-DEC-17
12978|Mount Norna Quartzite|69056|5|Briefly described|p4, p13, p55, Time-Space plot sheet|Statherian|Statherian|Soldiers Cap Domain. Detrital zircon maximum depositional age.|~1685 Ma (Neumann et al., 2009).|Soldiers Cap Group.||Is overlain by Toole Creek Volcanics possibly disconformably.|Meta-turbidites. Metamorphic grade increases from greenschist to gneiss and migmatites S of Snake Creek area.|
12978|Mount Norna Quartzite|69370|5|Briefly described|p307, p309, p311, p314-315|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block. Total thickness ca.2000 m; 150 m thick basal resistant feldspathic quartzite unit. Deformation described in detail.||Unit in Soldiers Cap Group.||Overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics.|Predominantly psammitic unit with minor poorly porphyroblastic pelitic intercalations.|25-JAN-19
12978|Mount Norna Quartzite|69591|4|Described|p38 Fig.2.22, p41, p43, p55|||Soldiers Cap Domain, Calvert Superbasin. Part of Prize and Gun Supersequences. Submarine fan deposits. Metamorphic grade increasing southwards into gneiss and migmatite. SHRIMP detrital zircon age.|1685 +/- 5 Ma (MDA: Neumann et al., 2009).|Soldiers Cap Group.||Overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics. Is intruded by Toole Creek Volcanics sills.|Fine-grained quartz sandstone, siltstone and mudstone; minor chert, limestone; grades into quartzite and schist. Characterised by bluish quartzite.|
12978|Mount Norna Quartzite|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics.|Fine-grained quartz sandstone, siltstone and mudstone; minor chert and limestone; grades into quartzite and schist; banded iron-formation.|
12978|Mount Norna Quartzite|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics.|Fine-grained quartz sandstone, siltstone and mudstone; minor chert and limestone; grades into quartzite and schist; banded iron-formation.|
12978|Mount Norna Quartzite|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Overlies Llewellyn Creek Formation. Is overlain by Toole Creek Volcanics.|Fine-grained quartz sandstone, siltstone and mudstone; minor chert, limestone; grades into quartzite and schist.|05-MAY-16
12978|Mount Norna Quartzite|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group.|||Fine grained quartz sandstone, siltstone and mudstone; minor chert, limestone; grades into quartzite and schist.|
12978|Mount Norna Quartzite|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group.|||Fine grained quartz sandstone, siltstone and mudstone; minor chert, limestone; grades into quartzite and schist.|20-JAN-22
12978|Mount Norna Quartzite|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group|||Fine grained quartz sandstone, siltstone and mudstone; minor chert, limestone grading into quartzite and schist.|
12978|Mount Norna Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1690+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Schist.|
12978|Mount Norna Quartzite|72889|5|Briefly described|p33, p35.|||||Soldiers Cap Group||Along with Llewellyn Creek Formation, correlated with Starcross Formation.||
12978|Mount Norna Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Snake Creek-Soldiers Cap Domain.|1654+/-4 Ma maximum depositional age||||Siliciclastics.|
12990|Mount Ox Subgroup|42249|6|Mentioned|Table 1 P22|||Reserved as Mount Ox||||||
12990|Mount Ox Subgroup|61612|6|Mentioned|p270 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||10-FEB-09
13019|Mount Peregian rhyolite|39969|6|Mentioned|Fig.22|||||||||
13019|Mount Peregian rhyolite|40542|6|Mentioned|p98|||||||||
13029|Mount Philp Breccia|24255|6|Mentioned|p44|||Geological Province: Mount Isa Block.||||||
13029|Mount Philp Breccia|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13029|Mount Philp Breccia|37862|4|Described|p586|||||||||
13029|Mount Philp Breccia|38238|4|Described|p135|||||||||
13029|Mount Philp Breccia|38350|4|Described|p19|||||||||
13029|Mount Philp Breccia|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13029|Mount Philp Breccia|39445|6|Mentioned|p43|||See also Table 2||||||
13029|Mount Philp Breccia|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
13029|Mount Philp Breccia|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Intrusive breccia.||||||09-FEB-09
13029|Mount Philp Breccia|45161|4|Described|p32|||See also Table 10||||||
13029|Mount Philp Breccia|45166|4|Described|p44|||||||||
13029|Mount Philp Breccia|49009|2|Defined|p29|Proterozoic|Proterozoic|Mapped as Mount Philp Agglomerate by Carter and others (1961).||||||01-FEB-07
13029|Mount Philp Breccia|49041|5|Briefly described|Table 2|||||||||
13029|Mount Philp Breccia|50100|5|Briefly described|p13 Fig. 4, p19|Statherian|Statherian|Intrudes the Corella Formation.  Geological Province: Eastern Fold Belt.||||||01-FEB-07
13029|Mount Philp Breccia|50332|5|Briefly described|p19|Proterozoic|Proterozoic|Intrudes Corella Formation. Consists of disoriented, angular to rounded fragments, Fragments include calc-silicate rocks, metasediments, metabasalt, metadolerite, qtz-feld pegmatite + leucogranite, + igneous textured groundmass.||||||07-FEB-11
13029|Mount Philp Breccia|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Intrusive breccia; some dolerite.||||||
13029|Mount Philp Breccia|60665|6|Mentioned|p1151 |||||||||
13029|Mount Philp Breccia|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Paleoproterozoic|Paleoproterozoic|Wonga/Burstall Igneous Event.||Wonga Suite, Burstall Suite|||Pink intrusive breccia containing abundant mafic clasts or xenoliths (and some calc-silicate rocks) in a dioritic matrix of albite laths and phenocrysts of amphibole, clinopyroxene and magnetite.|
13029|Mount Philp Breccia|69056|6|Mentioned|p13|||Combined with Corella Formation and Lime Creek Metabasalt for modelling purposes.||||||
13029|Mount Philp Breccia|69591|5|Briefly described|p60|||||Burstall Suite.|||Pink intrusive breccia with mafic clasts or xenoliths (and some calc-silicate rocks) in an altered dioritic matrix of albite, amphibole, clinopyroxene and magnetite.|
13029|Mount Philp Breccia|72596|5|Briefly described|p2-3, p28-38, p46|Calymmian|Calymmian|Geochronologic constraints are a maximum emplacement age from matrix zircons (1749 +/- 5 Ma), interpreted as inherited from the Corella Formation, and a titanite dominant age group of 1503 +/- 7 Ma, interpreted as a crystallisation age for the matrix and a probable emplacement age for the breccia. The probably emplacement age is similar to metamorphic zircon ages elsewhere. Lithologically similar to magmatic-hydrothermal breccias exposed elsewhere in the Eastern Fold Belt. Postdates regional deformation and amphibolite-grade metamorphism. Despite macro-textural similarities with igneous rock, matrix samples have a bulk geochemical composition unlike any known unaltered igneous rock, thus confirming the unit as a breccia. The Mount Philp Breccia is tentatively interpreted as a manifestation of widespread magmatic-hydrothermal activity associated with the Williams and Naraku Batholiths and may be associated with IOGC mineralisation.|1749 +/- 5 Ma and 1503 +/- 7 Ma, SHRIMP U-Pb|||Enclosed by the Corella Formation.|Polymictic, matrix-supported, magmatic-hydrothermal? breccia, consisting of randomly oriented, angular to rounded fragments and larger 'rafts' of country rocks dispersed in a pink to red or, more rarely grey, fine-grained matrix.|
13029|Mount Philp Breccia|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Intrusive breccia containing abundant mafic clasts or xenoliths (and some calc-silicate rocks) in a matrix of albitelaths and phenocrysts of amphibole, clinopyroxene and magnetite (highly altered hornblende diorite?).|
13029|Mount Philp Breccia|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mary Kathleen Domain, coaeval with the Wonga-Burstall Event (c. 1740 Ma).|c.1740 Ma.|Burstall Suite||Equivalent age to other Burstall Suite units and Wonga Suite units.|Intrusive breccia containing abundant mafic clasts or xenoliths (and some calc-silicate rocks) in a matrix of albitelaths and phenocrysts of amphibole, clinopyroxene and magnetite (highly altered hornblende diorite?).|
13029|Mount Philp Breccia|73413|6|Mentioned|p8, App.1|||U-Pb SHRIMP age of 1749 +/- 5 Ma and a metamorphic age of 1503 +/- 7 Ma were reported by Kositcin et al. (2019).||||||
13029|Mount Philp Breccia|73525|6|Mentioned|p4-5 Fig.2|||||||||
13029|Mount Philp Breccia|73553|4|Described|p3-4, p14, p37, p185-186,|Calymmian|Calymmian|Mary Kathleen Domain. Emplaced into Corella Formation, post-dates last major metamorphic event affecting the formation. Originally delineated as Mount Philp Agglomerate, name later changed to Mount Philp Breccia (Blake et al., 1981a, b). Spatially associated with IOCG-style mineralisation. Asssigned to the Burstall Suite by Hutton and Withnall (2013), discussed here that there is little justification for this. Mottled dark red tones on radiometric images, and a high magnetic response. See also p191-192, p195-196, p200, p213-214, p220-223.|1503+/-7 Ma U-Pb SHRIMP titanite, 1749+/-5 Ma MDA|Burstall Suite|||Resembles magmatic-hydrothermal explosion breccias, includes large inclusions and 'rafts' of unmetamorphosed but often metasomatised gabbro and metamorphosed country rocks.|03-FEB-23
13083|Mount Samson Granodiorite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
13083|Mount Samson Granodiorite|35007|6|Mentioned|p74|||||||||
13083|Mount Samson Granodiorite|35063|6|Mentioned|p79|||||||||
13083|Mount Samson Granodiorite|35430|6|Mentioned|Fig.2|||Geological map.||||||
13083|Mount Samson Granodiorite|35812|6|Mentioned|p568|||See also Fig.2||||||
13083|Mount Samson Granodiorite|36238|6|Mentioned|Table 1|||||||||
13083|Mount Samson Granodiorite|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early Triassic.||||||23-NOV-15
13083|Mount Samson Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
13083|Mount Samson Granodiorite|38074|6|Mentioned|Table 2|||||||||
13083|Mount Samson Granodiorite|39079|6|Mentioned|p9|||||||||
13083|Mount Samson Granodiorite|39445|5|Briefly described|Table 12|||||||||
13083|Mount Samson Granodiorite|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
13083|Mount Samson Granodiorite|43008|5|Briefly described|map legend|||||||||
13083|Mount Samson Granodiorite|43009|5|Briefly described|Map Legend|||||||||
13083|Mount Samson Granodiorite|43076|5|Briefly described|p6|||||||||
13083|Mount Samson Granodiorite|44814|14|Not recorded|p487|||||||||
13083|Mount Samson Granodiorite|44911|14|Not recorded|p2-4|||Outcrops across SE of resevoir area.||||||
13083|Mount Samson Granodiorite|44912|14|Not recorded|E12-B-7|||||||||
13083|Mount Samson Granodiorite|68679|5|Briefly described|p334, p427-428|Late Triassic|Late Triassic|Brisbane area.|217 Ma (K-Ar: Webb and McDougall, 1967).|||Intrudes Neranleigh-Fernvale beds and Bunya Phyllite.||
13083|Mount Samson Granodiorite|69952|5|Briefly described|p38|||||||Intrudes Neranleigh-Fernvale beds and Bunya Phyllite.||23-NOV-15
13144|Mount Tinbeerwah rhyolite|39969|6|Mentioned|Fig.22|||||||||
13144|Mount Tinbeerwah rhyolite|40542|6|Mentioned|p98|||||||||
13154|Mount Toussaint Volcanics|35940|5|Briefly described|p637|||||||||
13154|Mount Toussaint Volcanics|37612|6|Mentioned|p282|||||||||
13154|Mount Toussaint Volcanics|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|||||||
13154|Mount Toussaint Volcanics|44000|14|Not recorded|p24,25|||Ref. to Reid 1929. Former name for top unit of Lower Bowen Volcanics in Collinsville area; may be equivalent to Mount Devlin Volcanics.||||||
13154|Mount Toussaint Volcanics|44311|14|Not recorded|p195|||See also Lexicon.||||||
13154|Mount Toussaint Volcanics|44432|14|Not recorded|p44|||See also Lexicon.||||||
13154|Mount Toussaint Volcanics|44571|14|Not recorded|Fig.29|||See also Lexicon.||||||
13154|Mount Toussaint Volcanics|48626|14|Not recorded|p21|||See also Lexicon.||||||
13154|Mount Toussaint Volcanics|48881|14|Not recorded|p12|||Ref. to Reid 1924-1925,1929.||||||
13154|Mount Toussaint Volcanics|73029|5|Briefly described|Map legend|Early Permian|Early Permian|||Lizzie Creek Volcanic Group|||Basaltic to andesitic flows and volcaniclastic rocks ranging from siltstone to boulder conglomerate and breccia.|
13158|Mount Urah Granodiorite|24382|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|||||||
13158|Mount Urah Granodiorite|41736|6|Mentioned|p119|||Reserved as Urah||||||
13158|Mount Urah Granodiorite|41778|2|Defined|Table 3|Cretaceous|Jurassic|Reserved as Urah. Described P376.||||||14-AUG-08
13158|Mount Urah Granodiorite|42054|6|Mentioned|p272|||||||||
13158|Mount Urah Granodiorite|42894|5|Briefly described|p29|||||||||
13158|Mount Urah Granodiorite|43008|5|Briefly described|map legend|||||||||
13158|Mount Urah Granodiorite|63821|4|Described|p17, p33|Early Cretaceous|Late Jurassic|Age:140Ma. (K-Ar biotite).Intrudes Teebar + Brooweena Fms, Myrtle Creek Sst + Tiaro C.M. Zone of contact alteration at contact with Gigoomgan Limestone. Hornblende-biotite granodiorite, hornblende-pyroxene microdiorite + hornblende-biotite quartz diorite.||||||07-FEB-11
13158|Mount Urah Granodiorite|68553|6|Mentioned|Map legend|Cretaceous|Jurassic|This unit, as well as the Noosa Quartz Diorite, Mount Bauple Syenite, and unnamed intrusive units, are all mapped under the symbol, JKi.||||||
13158|Mount Urah Granodiorite|68679|6|Mentioned|p312|Cretaceous|Jurassic|Northern New England Orogen.||||||
13158|Mount Urah Granodiorite|69594|5|Briefly described|p549, p560-562|||Geochronology by Cranfield and Murray (1989).|140 +/- 1 Ma: K-Ar biotite.|||Intrudes Tiaro Coal Measures and Myrtle Creek Sandstone.|Includes a dominant hornblende-biotite granodiorite, pyroxene-hornblende microdiorite phase and a fine- to medium-grained porphyritic biotite granite phase.|
13158|Mount Urah Granodiorite|73422|6|Mentioned|p3, p7-8|Berriasian|Berriasian|[Also written as Mount Urah granodiorite]. Morton Igneous Association. New U-Pb zircon age of 140.7 +/- 0.7 Ma. Previous K-Ar age of ca. 140 Ma.|140.7 +/- 0.7 Ma U-Pb zircon|||||
13183|Mount Warner Volcanics|22482|4|Described|p487, p490||Middle Devonian|Of Capella Creek Group.||||||24-NOV-08
13183|Mount Warner Volcanics|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|Mount is Mt. in text.||||||
13183|Mount Warner Volcanics|24491|4|Described|p15|||Of Capella Creek Group. Overlies Mount Dick beds, overlain by Raspeberry Creek Formation. Divided into several informal units along the Dee Range, but not elsewhere.erent place.||||||
13183|Mount Warner Volcanics|24571|5|Briefly described|p8, 10|||Parent: Capella Creek beds.||||||24-NOV-08
13183|Mount Warner Volcanics|24615|5|Briefly described|CD|Middle Devonian|Middle Devonian|[Dcw].  Predominantly rhyolitic volcaniclastic sandstone and conglomerate, limestone, rhyolite, jasper.||||||
13183|Mount Warner Volcanics|40735|6|Mentioned|p1323|||||||||
13183|Mount Warner Volcanics|41824|6|Mentioned|p201|||||||||
13183|Mount Warner Volcanics|41983|6|Mentioned|p1809|||||||||
13183|Mount Warner Volcanics|42868|5|Briefly described|p20|||actually spelt Mt Warner Volcanics||||||
13183|Mount Warner Volcanics|50208|5|Briefly described|Map Legend|Devonian|Devonian|Of the Capella Creek Group.||||||
13183|Mount Warner Volcanics|50317|5|Briefly described|Map Legend|Devonian|Devonian|Of the Capella Creek Group.||||||09-JUN-04
13183|Mount Warner Volcanics|61147|5|Briefly described|pp375-377, p379.   |||Dee Range. Correlation with the Banded Mine Sequence of the Mount Morgan copper-gold deposit suggests this unit may be similarly prospective.||Unit in Capella Creek Group.|Includes "Banded Mineralised Sequence".|Intruded by Mount Morgan trondhjemite and Bouldercombe Complex. Overlies the Mount Dick beds.|Quartz-rich sediments and breccia; acid lavas, jasper, peperite, limestone; altered andesitic breccias and sediments; mineralised.|
13183|Mount Warner Volcanics|61730|5|Briefly described|p1001|Eifelian|Eifelian|Of the Capella Creek Group. Dominated by sediments sourced from dacitic and rhyolitic volcanic rocks; abundant pumice clasts and rare limestone lenses. Intruded by Mount Morgan Trondhjemite from which this unit is indistinguishable. Mount is Mt in text||||||
13183|Mount Warner Volcanics|61808|5|Briefly described|p446, p447 Fig. 1|Middle Devonian|Late Silurian|Mount is Mt in text. Of Capella Creek Group. May correlate to Mine Corridor Volcanics.||||||
13183|Mount Warner Volcanics|63600|5|Briefly described|p917|Middle Devonian|Middle Devonian|Middle unit of Capella Creek Group. Mount is Mt in text.||||||07-FEB-11
13183|Mount Warner Volcanics|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Mount Morgan. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
13183|Mount Warner Volcanics|68008|1|Redefined|p16, p26-27, p29-34, p36, p40, p318,p395|Middle Devonian|Middle Devonian|See also p487-488, p573, p576-579, p601. Originally the lower, silicic part of the Capella Creek beds of Kirkegaard et al. (1970). Separated as a unit by Taube (1986), but subsumed into the Capella Creek Formation of Morand (1993). Redefined as Mount Warner Volcanics, with three informal sub-units, by Messenger and Taube (1994); later included as part of the Capella Creek Group by the Yarrol Project Team (1997). Named after Mount Warner (labelled Mount Dick on the 100k topographic map). The type section is along the road to the Mount Hopeful TV towers, where it is almost 1000m thick (1900m at Mount Morgan). Crops out along the crest of the Dee Range, and as a roof pendant (formerly known as the Mine Corridor Volcanics) in the Mount Morgan Trondhjemite. There it comprises massive crystal-rich pumiceous volcaniclastic mass-flow deposits with lesser jasper, tuffaceous mudstone, siltstone and sandstone, limestone lenses/bands, and domes or lava flows of quartz-feldspar porphyries. Hosts the Mount Morgan Au-Cu deposit. Forms high, rugged topography. Geochemistry detailed: likened to Mount Morgan Trondhjemite (co-genetic) and contrasted with that of Craigilee beds. Eifelian age from conodonts.||Capella Creek Group.||Conformably overlies Mount Dick beds. Is overlain conformably by Raspberry Creek Formation. Is intruded by Bajool Quartz Diorite. Correlated with Mine Corridor Volcanics.|Sandstone and granule to pebble breccia (andesitic to basaltic sources); a locally-interbedded succession of rhyolite lava, sandstone, jasper, siltstone and rare peperite (rhyolitic source); sandstone, conglomerate and rare limestone.|
13183|Mount Warner Volcanics|68679|5|Briefly described|p315-316, p401, p403 Tb.5.8, p425|Eifelian|Eifelian|Taube (1986); Messenger and Taube (1994). Originally the lower part of the Capella Creek beds. Forms a SE-trending belt 30km long and up to 4km wide along the Dee Range, from Moongan to S of Mount Hopeful; also includes the former Mine Corridor Volcanics, a roof pendant in the Mount Morgan Trondhjemite, that hosts the Mount Morgan Au-Cu deposit (origin discussed). Is geochemically indistinguishable from the Mount Morgan Trondhjemite, but is ~15my older. Island arc environment.||Capella Creek Group.||Overlies Mount Dick beds. Is intruded by Bajool Quartz Diorite.|Basal sandstone and granule to pebble conglomerate sourced from mafic rocks; overlain by sandstone (sourced from rhyolitic volcanics and granitoids), siltstone, jasper, rhyolite with rare peperite and micritic, fossiliferous (corals) limestone.|
13184|Mount Warning Central Complex|22773|6|Mentioned|p343|||||||||
13184|Mount Warning Central Complex|22857|5|Briefly described|p345|||At the centre of the Tweed volcano in the central-volcano provinces of NSW.||||||
13184|Mount Warning Central Complex|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|30131|4|Described|p10|||See also P8||||||
13184|Mount Warning Central Complex|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|34340|6|Mentioned|p476|||||||||
13184|Mount Warning Central Complex|34755|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|40896|4|Described|p10|||||||||
13184|Mount Warning Central Complex|43161|4|Described|12-18|||K-Ar Dates: 22.9, 23.7 Ma. Aged: 23.4 Ma||||||
13184|Mount Warning Central Complex|43881|14|Not recorded|p53,72,170|Tertiary|Early Triassic|||||||
13216|Mount Wickham Rhyolite|22675|4|Described|p157 App.1|Triassic|Permian|230+/-15Ma, Bowen Basin||||||
13216|Mount Wickham Rhyolite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 225. Assumed to be I-Type.||||||
13216|Mount Wickham Rhyolite|30914|6|Mentioned|Map legend|Triassic|Permian|Permian - Triassic||||||
13216|Mount Wickham Rhyolite|31984|6|Mentioned|Map legend|Early Triassic|Late Permian|U.Permian to L.Triassic||||||
13216|Mount Wickham Rhyolite|32553|4|Described|p40|||||||||
13216|Mount Wickham Rhyolite|32556|4|Described|Table 4|||U.Perm.-L.Trias.||||||
13216|Mount Wickham Rhyolite|35940|5|Briefly described|p639|||||||||
13216|Mount Wickham Rhyolite|36472|6|Mentioned|Map legend|Triassic|Late Permian|Triassic to Late Permian||||||
13216|Mount Wickham Rhyolite|37613|5|Briefly described|p249|||See also Fig.3||||||
13216|Mount Wickham Rhyolite|39445|5|Briefly described|Table 9|||||||||
13216|Mount Wickham Rhyolite|40574|6|Mentioned|p4|||||||||
13216|Mount Wickham Rhyolite|40787|6|Mentioned|p373|||||||||
13216|Mount Wickham Rhyolite|41246|6|Mentioned|Map legend|Triassic|Permian|||||||
13216|Mount Wickham Rhyolite|43259|4|Described|Appendix 1,p32.|Early Triassic|Late Permian|Upper Permian to Lower Triassic?.||||||
13216|Mount Wickham Rhyolite|43391|5|Briefly described|Map legend|Permian|Permian|Geological Province: Bowen Basin.  Intrusive rhyolite and probable lava.||||||23-JUN-04
13216|Mount Wickham Rhyolite|43706|5|Briefly described|p15|||||||||
13216|Mount Wickham Rhyolite|45151|5|Briefly described|Table 10|||||||||
13216|Mount Wickham Rhyolite|48922|3|Fully described|p51|||230 +/- 15m.y.||||||
13216|Mount Wickham Rhyolite|60659|5|Briefly described|p20|||Extrusive and intrusive rocks, unconformable over Lizzie Creek Volcanic Group, Mount Windsor Volcanics and Scartwater Formation. Geological Province: Bowen Basin.||||||29-APR-13
13216|Mount Wickham Rhyolite|65706|4|Described|p9 Fig.3; Tb.1 p15,16,17; p23,p42 Fig.10|Early Triassic|Middle Permian|See also p51, p54, p81, p87-9, p93, p95, p119-20, p123, p130, p150. Hosts disseminated epithermal Au mineralisation.||||Intrudes and unconformably overlies Lizzie Creek Volcanic Unit and Mount Windsor Volcanics.|Mainly flow-banded porphyritic rhyolite, rhyolitic breccia, with subordinate trachyte, dacite, obsidian and agglomerate.|
13216|Mount Wickham Rhyolite|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Connors Subprovince. This unit is mapped with Lizzie Creek Volcanic Group under the symbol, Pvz.||||||
13216|Mount Wickham Rhyolite|68679|5|Briefly described|p312-313, p361, p364, p368|Permian|Permian|Northern New England Orogen. Other similar ages given.|285 +2/-1 Ma: U-Pb SHRIMP: Cross et al. (2012).|||||
13216|Mount Wickham Rhyolite|68901|4|Described|p2-4, p68-72, p106-109|Permian|Permian|northern New England Orogen, Bowen Region. Relatively well exposed. Previous Rb-Sr whole rock age: 230+/-15 Ma (Webb& McDougall,  1968). 2 samples dated, both flowbanded rhyolites. Dates are SHRIMP U-Pb ages and interpreted as the date of magmatic crystallisation. SHRIMP results and analysis discussed in detail. See also p98, p102, p118, p145, p146.|285 +2/-1 Ma and 286.6 +/- 2.2 Ma|||Interlayered with and intrudes the Lizzie Creek Volcanic Group.|Pale-grey to pale pinkish grey, very fine-grained, slightly poprhyritic rhyolite containing scattered phenocrysts of K-feldspar. Commonly flow banded, autobrecciated and slightly to moderately altered.|04-OCT-18
13216|Mount Wickham Rhyolite|69952|6|Mentioned|p85|Permian|Permian|New England Orogen.||||||
13216|Mount Wickham Rhyolite|70740|6|Mentioned|p124|||||||||
13216|Mount Wickham Rhyolite|70837|5|Briefly described|p246|Cisuralian|Cisuralian|Of  Bowen Basin. SHRIMP ages of 285 and 286.6 (Cross etal., 2012). Corresponding to APP3 zone (Cisuralian-Guadalupian).||Unit of Lizzie Creek Volcanic Group.||||
13216|Mount Wickham Rhyolite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|285 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
13235|Mount Windsor Volcanics|22543|6|Mentioned|p62|Early Ordovician|Late Cambrian|assigned to the Thalanga Province||||||
13235|Mount Windsor Volcanics|22621|5|Briefly described|p204|Ordovician|Cambrian|Part of Seventy Mile Range Group.||||||10-FEB-09
13235|Mount Windsor Volcanics|22628|6|Mentioned|p112|Cambrian|Cambrian|spelt "Mt" in the text||||||
13235|Mount Windsor Volcanics|22675|4|Described|p13|||||||||
13235|Mount Windsor Volcanics|22708|6|Mentioned|p209|||||||||
13235|Mount Windsor Volcanics|22847|5|Briefly described|p 6|Arenig|Arenig|||||||
13235|Mount Windsor Volcanics|23032|6|Mentioned|p14|||||||||
13235|Mount Windsor Volcanics|23074|5|Briefly described|p737|Ordovician|Cambrian|||||||
13235|Mount Windsor Volcanics|23402|5|Briefly described|p45|||Geological Province: Tasman Fold Belt||||||
13235|Mount Windsor Volcanics|23422|4|Described|p170, p206 Table 6.3|Middle Ordovician|Cambrian|Of Seventy Mile Range Group.  Overlain by Trooper Creek Formation. Underlain by Puddler Creek Formation.||||||10-FEB-09
13235|Mount Windsor Volcanics|23430|4|Described|p469-470|||Of Seventy Mile Creek Group. Underlain by Puddler Creek Formation - conformable. Thalanga Province.||||||10-FEB-09
13235|Mount Windsor Volcanics|23431|5|Briefly described|p537|||Written as 'Mt' in text.  Of Seventy Mile Range Group.||||||10-FEB-09
13235|Mount Windsor Volcanics|23504|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||10-FEB-09
13235|Mount Windsor Volcanics|23505|5|Briefly described|Map legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||10-FEB-09
13235|Mount Windsor Volcanics|23513|5|Briefly described|Map legend|Ordovician|Ordovician|Palaeozoic Volcanic No. V67. Assumed to be I-Type.||||||
13235|Mount Windsor Volcanics|23942|6|Mentioned|p965|||||||||
13235|Mount Windsor Volcanics|23951|6|Mentioned|p1149|||||||||
13235|Mount Windsor Volcanics|23954|5|Briefly described|p1227|Ordovician|Cambrian|||||||
13235|Mount Windsor Volcanics|23986|6|Mentioned|p100|||Mount is Mt. in text.||||||
13235|Mount Windsor Volcanics|23988|5|Briefly described|p15|Cambrian|Cambrian|Of Seventy Mile Range Group.||||||
13235|Mount Windsor Volcanics|24035|5|Briefly described|p2, p3 Fig. 1, p6 Fig. 3, p13 Fig. 18|Early Ordovician|Cambrian|Of Seventy Mile Range Group. Mount is Mt in text. Rhyolite, volcaniclastics and some andesite.||||||
13235|Mount Windsor Volcanics|24168|6|Mentioned|p643|||||||||
13235|Mount Windsor Volcanics|24263|5|Briefly described|p1383 Fig.2|Early Ordovician|Late Cambrian|||||||
13235|Mount Windsor Volcanics|24290|6|Mentioned|p910|||||||||
13235|Mount Windsor Volcanics|24424|5|Briefly described|p524|Early Ordovician|Late Cambrian|Of 70 Mile Group. Geological Province: Lolworth-Ravenswood Province.||||||04-FEB-05
13235|Mount Windsor Volcanics|30148|4|Described|Table 1|||Cambrian - Ordovician age.||||||
13235|Mount Windsor Volcanics|30149|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician age||||||
13235|Mount Windsor Volcanics|30151|4|Described|Table 1|||Cambrian - Ordovician age.||||||
13235|Mount Windsor Volcanics|30914|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
13235|Mount Windsor Volcanics|31813|6|Mentioned|Table 2|||Pre-Silurian||||||
13235|Mount Windsor Volcanics|31984|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian-Ordovician||||||
13235|Mount Windsor Volcanics|31999|6|Mentioned|p127|||See also P141, Table 11||||||
13235|Mount Windsor Volcanics|32493|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
13235|Mount Windsor Volcanics|32553|4|Described|p54|||||||||
13235|Mount Windsor Volcanics|32556|4|Described|Table 2|||Cambrian to Ordovician ?||||||10-FEB-09
13235|Mount Windsor Volcanics|34408|6|Mentioned|p185|||On Table||||||
13235|Mount Windsor Volcanics|34409|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian - Ordovician||||||
13235|Mount Windsor Volcanics|35154|6|Mentioned|p305|||||||||
13235|Mount Windsor Volcanics|35304|6|Mentioned|p605|||||||||
13235|Mount Windsor Volcanics|36472|6|Mentioned|Map legend|Ordovician|Cambrian|Ordovician to Cambrian||||||
13235|Mount Windsor Volcanics|36561|6|Mentioned|Fig.1|||||||||
13235|Mount Windsor Volcanics|37570|6|Mentioned|p123|||||||||
13235|Mount Windsor Volcanics|37764|6|Mentioned|Table 1|||||||||
13235|Mount Windsor Volcanics|37765|5|Briefly described|p9|||||||||
13235|Mount Windsor Volcanics|37768|6|Mentioned|p40|||||||||
13235|Mount Windsor Volcanics|39445|6|Mentioned|p62|||See also P66 & Table 4||||||
13235|Mount Windsor Volcanics|39686|6|Mentioned|p69|||||||||
13235|Mount Windsor Volcanics|39689|6|Mentioned|Fig.4|||||||||
13235|Mount Windsor Volcanics|39734|6|Mentioned|p22|||||||||
13235|Mount Windsor Volcanics|39735|6|Mentioned|p16|||||||||
13235|Mount Windsor Volcanics|39995|6|Mentioned|p217|||||||||
13235|Mount Windsor Volcanics|40128|6|Mentioned|p2|||||||||
13235|Mount Windsor Volcanics|40136|5|Briefly described|p33|||||||||
13235|Mount Windsor Volcanics|40623|5|Briefly described|p110|||||||||
13235|Mount Windsor Volcanics|40746|3|Fully described|p347|||||||||
13235|Mount Windsor Volcanics|40787|6|Mentioned|p322|||||||||
13235|Mount Windsor Volcanics|40915|5|Briefly described|p113|||||||||
13235|Mount Windsor Volcanics|40958|6|Mentioned|p160|||||||||
13235|Mount Windsor Volcanics|40974|6|Mentioned|p204|||||||||
13235|Mount Windsor Volcanics|41246|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
13235|Mount Windsor Volcanics|41272|6|Mentioned|M 1of1 E10|||||||||
13235|Mount Windsor Volcanics|41675|5|Briefly described|p31|||||||||
13235|Mount Windsor Volcanics|41805|6|Mentioned|Fig.2|||||||||
13235|Mount Windsor Volcanics|42216|5|Briefly described|p423|||||||||
13235|Mount Windsor Volcanics|42245|5|Briefly described|p34|||||||||
13235|Mount Windsor Volcanics|42279|5|Briefly described|p17|||||||||
13235|Mount Windsor Volcanics|42398|5|Briefly described|Fig.1 PB1|||||||||
13235|Mount Windsor Volcanics|42633|4|Described|p15|||||||||
13235|Mount Windsor Volcanics|42750|6|Mentioned|p35|||||||||
13235|Mount Windsor Volcanics|42986|5|Briefly described|p393|||||||||
13235|Mount Windsor Volcanics|43093|5|Briefly described|p14|||Of Seventy Mile Range Group.||||||10-FEB-09
13235|Mount Windsor Volcanics|43128|5|Briefly described|p473,p476.|||Distinct from Mt Windsor Formation,also p476.||||||
13235|Mount Windsor Volcanics|43259|4|Described|Appendix 1,p6.|Ordovician|Cambrian|Age: Upper Cambrian to Lower Ordovician.||||||17-JUL-14
13235|Mount Windsor Volcanics|43391|5|Briefly described|Map legend|Ordovician|Cambrian|Of the Seventy Mile Range Group.    Mainly rhyolites of uncertain origins.||||||23-JUN-04
13235|Mount Windsor Volcanics|43567|6|Mentioned|p397|Carboniferous|Devonian|||||||
13235|Mount Windsor Volcanics|43706|5|Briefly described|p14|||||||||
13235|Mount Windsor Volcanics|43727|6|Mentioned|Fig.1,p1||Paleoproterozoic|||||||07-NOV-08
13235|Mount Windsor Volcanics|43763|6|Mentioned|p744|||||||||
13235|Mount Windsor Volcanics|43766|6|Mentioned|p920|||||||||
13235|Mount Windsor Volcanics|43772|6|Mentioned|p785|Late Ordovician|Cambrian|||||||
13235|Mount Windsor Volcanics|43934|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
13235|Mount Windsor Volcanics|43936|5|Briefly described|Map Legend|Ordovician|Cambrian|Of Seventy Mile Range Group.||||||
13235|Mount Windsor Volcanics|43994|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
13235|Mount Windsor Volcanics|44337|5|Briefly described|Map Legend||Paleoproterozoic|Lithology.||||||07-NOV-08
13235|Mount Windsor Volcanics|45071|5|Briefly described|p11|||Age: 345-372 m.y.||||||10-FEB-09
13235|Mount Windsor Volcanics|45151|6|Mentioned|p4|||||||||
13235|Mount Windsor Volcanics|46899|6|Mentioned|p11|||Heat flow||||||
13235|Mount Windsor Volcanics|48914|3|Fully described|p16|||See also p17. Cambrian - Ordovician.||||||10-FEB-09
13235|Mount Windsor Volcanics|48922|4|Described|p14|||See also p10. Upper Cambrian.||||||10-FEB-09
13235|Mount Windsor Volcanics|48951|6|Mentioned|p8|||||||||
13235|Mount Windsor Volcanics|50153|6|Mentioned|p2,p15|||Host for volcanigenic Cu-Pb-Zn-Ag-Au-Ba mineralisation||Of the Seventy Mile Range Group||||28-MAR-12
13235|Mount Windsor Volcanics|60659|5|Briefly described|p10, p90|||Thick sequence of rhyolitic to dacitic volcanic rocks, including volcaniclastics and minor andesite. Overlain by Trooper Creek Formation; unconformably overlain by Mount Wickham Rhyolite.||||||07-FEB-11
13235|Mount Windsor Volcanics|61187|5|Briefly described|pp14-15, p23. |Ordovician|Late Cambrian|Hosts the Thalanga VHMS deposit. Occupies a similar position, adjacent to the Tasman Line, as Mount Stavely Volcanic Complex (Victoria) and Mount Read Volcanics (Tasmania).||||||
13235|Mount Windsor Volcanics|62079|6|Mentioned|p43|Ordovician|Cambrian|Hosts VMS base-metal deposits.||Unit in Trooper Creek Formation||||
13235|Mount Windsor Volcanics|62521|5|Briefly described|p1, p47|Middle Ordovician|Late Cambrian|Geological Province: Ravenswood Batholith.||||||14-JAN-08
13235|Mount Windsor Volcanics|64850|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Acid to intermediate volcanics (lava and volcaniclastics), sandstone, schist, hornfels.||||||09-FEB-09
13235|Mount Windsor Volcanics|64852|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Seventy Mile Range Group. Acid to intermediate volcanics (lava and volcaniclastic), sandstone, schist, hornfels.||||||
13235|Mount Windsor Volcanics|65706|4|Described|p10; Tb.1 p13,16; p45, p48-49, p54, p55|Early Ordovician|Late Cambrian|See also p60, p66, p104, p107, p126, p128, p131, p133-4, p136, p146, p148. Hosts Landers Creek Prospect Cu-Pb-Zn-Ag deposit; gold-bearing quartz veins and stockwork at the Sullivans Reward (Six Mile Bore) Prospect; gold+sulfides at Mount Glenroy Prospect; gold at the Pinnacle (Old Rangeview), Gold Creek and Three Peaks Prospects; Au-Ag-base metals.||Of Seventy Mile Range Group.||Intruded and metamorphosed by Ravenswood Granodiorite Complex. Unconformable under Bulgonunna Volcanic Group; intruded and unconformably underlain by Mount Wickham Rhyolite.|Acid to intermediate volcanics (lavas and volcaniclastics), sandstone, schist, quartzite, phyllite, hornfels.|
13235|Mount Windsor Volcanics|66860|6|Mentioned|p65|||Cited as an example of metamorphosed, carbonate-bearing rocks associated with VAMS.||||||
13235|Mount Windsor Volcanics|68731|5|Briefly described|p145, p146, p147, p152, p155, p159, p220|Early Ordovician|Late Cambrian|Henderson (1986). Southern Charters Towers Province. Thins to the west.||Of the Seventy Mile Range Group.|||Comprises a thick succession of rhyolitic to dacitic lavas, autoclastic and reworked breccia facies, and minor andesite and sedimentary rocks.|
13235|Mount Windsor Volcanics|68900|4|Described|p11-p13|Early Ordovician|Early Ordovician|Originally designated by Wyatt et al (1971) to the Cape River beds. Confined in the study area to the northern part of HARVEST HOME and PAJINGO map sheets. This unit is generally resistant to weathering and forms hills. Deposited in a subaqueous, probably deep water environment in a back-arc extensional setting. Between 1000 and 3500m thick.|479 +/- 5 Ma (SHRIMP U-Pb, Perkins et al, 1995)|Seventy Mile Range Group||Conformably overlies the Puddler Creek Formation. Conformably overlain by the Trooper Creek Formation.|Rhyolite, rhyolite porphyry, dacite and minor andesite, basalt, pyroclastics and interbedded sediments.|
13235|Mount Windsor Volcanics|69952|5|Briefly described|p4|Early Ordovician|Early Ordovician|Age by Perkins (1995) in Henderson and Hutton (2013).|479 +/- 5 Ma (SHRIMP U-Pb zircon).|Unit in Seventy Mile Range Group.||Overlies Puddler Creek Formation.||30-NOV-15
13235|Mount Windsor Volcanics|70207|5|Briefly described|p1, p11, p33, p38-44|||Charters Towers Province, Thomson Orogen. Doubt about the sample being Puddler Creek Formation discussed. Maximum depositional age; consistent with graptolite and magmatic age constraints elsewhere in the Seventy Mile Range Group. Detrital age spectrum is similar to that of Les Jumelles beds.|498.7 +/- 5.8 Ma (Kositcin et al., 2015).|Seventy Mile Range Group.|||A thick succession of marine rhyolite lavas and breccias, minor andesitic volcanics, and minor sedimentary rocks including sublithic sandstone.|
13235|Mount Windsor Volcanics|70345|5|Briefly described|p19|||Charters Towers Province of the Thomson Orogen.|479 +/- 5 Ma (SHRIMP U-Pb)||||Volcanic rocks includoing rhyolite.|
13235|Mount Windsor Volcanics|70740|5|Briefly described|p36-p37, p78|Early Ordovician|Early Ordovician|Basement unit in the northeastern Drummond Basin. Outcrop characteristics discussed. Age derived from Perkins et al., 1993. Informally subdivided into five units on the basis of lithology. Hosts important VHMS deposits.||Seventy Mile Range Group||Unconformably overlain by the Stones Creek Volcanics. Overlain by the Scartwater Formation, Star of Hope Formation, Bulgonunna Volcanic Group.|Pale grey to greenish grey, sparsely porphyritic rhyolite with local flow banding and spherulites. Fragmental andesite, dacite and rhyolite also occur.|
13235|Mount Windsor Volcanics|70749|4|Described|p43, p45-48, p51-52|Ordovician|Ordovician|Charters Towers Province. Another age determination of 479 +/- 5 Ma is given, but is suspected of Pb loss.|499 +/- 6 Ma (maximum deposition age).|Seventy Mile Range Group.||Is overlain by Trooper Creek Formation.|Medium-grained sublithic sandstone.|
13235|Mount Windsor Volcanics|71031|4|Described|p3, p6, p44, p50, p53, p62, p77|Ordovician|Ordovician|Charters Towers Province. Ages are SHRIMP U-Pb dates and interpreted as magmatic crystallisation ages; these ages are within error of a U-Pb zircon SHRIMP date of 479 +/- 5 Ma reported in Perkins et al (1993). See also the informal Mount Windsor rhyolite.|481.5 +/- 2.7 Ma and 482.1 +/- 3|||Intruded by the Mount Glenroy microgranite.|Altered and brecciated rhyolite.|
13235|Mount Windsor Volcanics|71965|6|Mentioned|p911|||Geological province: Thomson Orogen.||||Correlable to Warratta Group.||
13235|Mount Windsor Volcanics|71966|6|Mentioned|p990|Tremadocian|Tremadocian|Geological province: Charters Towers Province, Thomson Orogen.|479+\-5 Ma (SHRIMP U-PB)|||||
13235|Mount Windsor Volcanics|73425|6|Mentioned|p18||||479 +/- 5 Ma.|Seventy Miles Range Group.||||
13251|Mount Wyatt Formation|22675|4|Described|p19|Late Devonian|Late Devonian|Drummond Basin||||||
13251|Mount Wyatt Formation|22800|3|Fully described|Fig.14 p592, p580|Famennian|Famennian|Spelt Mt Wyatt Formation. See also p581, Fig.4 p583||||||
13251|Mount Wyatt Formation|23052|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
13251|Mount Wyatt Formation|23161|4|Described|p12,13 table 2a|Early Carboniferous|Middle Devonian|||||||
13251|Mount Wyatt Formation|23430|5|Briefly described|Plate 14.11 + p510|Early Carboniferous|Late Devonian|Drummond Basin Province.||||||
13251|Mount Wyatt Formation|23986|6|Mentioned|p104|||Mount is Mt. in text.||||||
13251|Mount Wyatt Formation|23988|5|Briefly described|p50|||Mount is Mt. in text.||||||
13251|Mount Wyatt Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Late Devonian|Sandstone, conglomerate, siltstone, mudstone and tuff.  Max. thickness: 150m.  Geological Province: Drummond Basin.||||||
13251|Mount Wyatt Formation|24613|6|Mentioned|p77, p135|Late Devonian|Late Devonian|Geological province: Drummond Basin. Contains brachiopods.||||||07-FEB-11
13251|Mount Wyatt Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
13251|Mount Wyatt Formation|31984|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
13251|Mount Wyatt Formation|31999|5|Briefly described|p136|||See also Fig. 2, Table 1||||||
13251|Mount Wyatt Formation|32493|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
13251|Mount Wyatt Formation|32553|4|Described|p50|||||||||
13251|Mount Wyatt Formation|32556|4|Described|Table 2|||U.Dev.||||||
13251|Mount Wyatt Formation|32619|6|Mentioned|p463|||U. Dev.||||||
13251|Mount Wyatt Formation|32865|4|Described|p482|||Late Devonian - early Carboniferous||||||
13251|Mount Wyatt Formation|36472|6|Mentioned|Map legend|Late Devonian|Middle Devonian|Middle to Late Devonian||||||
13251|Mount Wyatt Formation|37565|6|Mentioned|Fig.8|||||||||
13251|Mount Wyatt Formation|37573|4|Described|p223|||||||||
13251|Mount Wyatt Formation|39212|6|Mentioned|p6|||||||||
13251|Mount Wyatt Formation|39445|5|Briefly described|Table 6|||See also P82. Marine||||||
13251|Mount Wyatt Formation|41246|6|Mentioned|Map legend|Devonian||||||||
13251|Mount Wyatt Formation|41272|6|Mentioned|M 1of1 M11|||||||||
13251|Mount Wyatt Formation|42486|5|Briefly described|p201|||||||||
13251|Mount Wyatt Formation|42547|5|Briefly described|p60|||Actually spelt Mt Wyatt Formation||||||
13251|Mount Wyatt Formation|42678|6|Mentioned|p246|||||||||
13251|Mount Wyatt Formation|42701|4|Described|p22|||||||||
13251|Mount Wyatt Formation|43105|6|Mentioned|p12|||||||||
13251|Mount Wyatt Formation|43213|5|Briefly described|p67, p74|Late Devonian|Late Devonian|Among the oldest rocks in north Drummond Basin. Marine deposition. Interpreted as a near-shore to paralic equivalent of the Campwyn beds (Yarrol Province).||||Correlated with Myrtlevale Formation (Burdekin Basin).|Includes volcanilithic rocks.|
13251|Mount Wyatt Formation|43391|5|Briefly described|Map legend|Late Devonian|Late Devonian|Geological Province: Drummond Basin.  Mainly mudstone and sandstone; subsidiary conglomerate.||||||23-JUN-04
13251|Mount Wyatt Formation|43706|5|Briefly described|p12||Late Devonian|||||||
13251|Mount Wyatt Formation|44081|14|Not recorded|p107,113,Fig.6,155-6|||p161||||||
13251|Mount Wyatt Formation|44245|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
13251|Mount Wyatt Formation|45073|3|Fully described|p24|||||||||
13251|Mount Wyatt Formation|45151|5|Briefly described|Table 6|||||||||
13251|Mount Wyatt Formation|48922|4|Described|p13|||||||||
13251|Mount Wyatt Formation|60659|4|Described|p11, p58|Early Carboniferous|Late Devonian|Mainly sedimentary, shallow marine and paralic environment deposits. Unconformably overlie Bimurra Volcanics; unconformably overlain by Bulgonunna Volcanic Group. Intruded by Sunbeam Granodiorite. Geological Province: Drummond Basin.||||||07-FEB-11
13251|Mount Wyatt Formation|64783|6|Mentioned|p102|Famennian|Famennian|Marine transgression in northern Drummond Basin.||||||15-NOV-17
13251|Mount Wyatt Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Bimurra, Foyle, Silver Hills and Stones Creek Volcanics, and the Saint Anns Formation, are all mapped under the symbol, DCD1.||||||
13251|Mount Wyatt Formation|68679|6|Mentioned|p364|Early Carboniferous|Late Devonian|||||||
13251|Mount Wyatt Formation|68731|5|Briefly described|p128, p172, p191 Fig 3.102, p192, p193|Late Devonian|Late Devonian|Drummond Basin.||||Overlain by Les Jumelles beds; conformably by Saint Anns Formation and Bimurra Volcanics in the far north; disconformably by Ukalunda Formation. Overlies Bimurra Volcanics in southwest BOWEN area.||11-MAY-16
13251|Mount Wyatt Formation|68900|5|Briefly described|p4, p18, p23, p27, p30-p31, p43-p44, p57|Late Devonian|Late Devonian|Drummond Basin.||||Unconformably overlies the Les Jumelles beds. Overlies the Ukalunda Formation. Overlain by the Saint Anns Formation (probably gradationally).||
13251|Mount Wyatt Formation|68901|5|Briefly described|p2, p114|Early Carboniferous|Late Devonian|Drummond Basin.||||Overlain by the Pyramid Rhyolite.||27-SEP-18
13251|Mount Wyatt Formation|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|||||||
13251|Mount Wyatt Formation|70740|3|Fully described|i, ii, p1, p7, p20, p24, p27|Famennian|Famennian|Drummond Basin. Large parts of this unit were remapped as the Bimurra Volcanics in this volume. A type area is given from Olgers (1972) and a type section is mentioned from Henderson et al., 1998. Previously named the "Mount Wyatt beds" (Daintree., 1870 and Malone et al., 1966) before being raised to formation status by Olgers (1972). Only unit in the Drummond Basin that contains marine fossils -these are the basis for this formations age determination. Thickness of this unit is unclear and is variably proposed to be up to 1500m or as low as no more than 500m. Lithology at the type section is described in detail. Structure, boundary criteria are discussed. Often difficult to distinguish from the Bimurra Volcanics. Unconformably overlain by the Bulgonunna Volcanic Group. Part equivalent of the Bimurra Volcanics and the Mount Hoopbound Formation. Equivalent to the Myrtlevale Formation. Intruded by the Sunbeam Granodiorite, Percy Douglas Tonalite and Wynne Creek Diorite. See also p33-p35, p41-p44, p46-p49, p51-p52, p55, p66, p72, p73, p76, p80, p81, p128, p130.||||Unconformably overlies the Les Jumelles beds. Disconformably overlies the Ukalunda Formation. Conformably overlain by the Bimurra Volcanics and the the Saint Anns Formation.|Green, khaki and grey shale, siltstone and lithic sandstone with some thin conglomerate interbeds containing granite and quartz clasts.|
13251|Mount Wyatt Formation|73198|5|Briefly described|p499-500, p510-511, p514 Fig.18|||[Written as Mt Wyatt Formation]. Drummond Basin, north. Part of Cycle 1 of Olgers (1972). Records basin-wide contemporaneous volcanism. Maximum thickness: 1500 m. Volcanic provenance. [See article for petrographic descriptions and data].||||Overlain by Saint Anns Formation.||02-NOV-22
13259|Mountain Creek Conglomerate|23423|4|Described|p302 Table 7.2||Late Ordovician|Age: 455 +/- 5 Ma (SHRIMP). Faulted against the Mulgrave Formation. Also see p231. Underlying unit Chillagoe Formation (unconformable).||||||
13259|Mountain Creek Conglomerate|23424|5|Briefly described|p345|||Probably correlate with Everetts Creek Volcanics and Carriers Well Formation. Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|23430|4|Described|p471-473|||Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|23431|6|Mentioned|p539|||Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|23511|5|Briefly described|Map Legend||Late Ordovician|||||||
13259|Mountain Creek Conglomerate|23616|5|Briefly described|p29|||Underlying Unit Mulgrave Formation - unconformable. Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|23713|5|Briefly described|p13||Late Ordovician|||||||
13259|Mountain Creek Conglomerate|24485|5|Briefly described|p27|Late Ordovician|Late Ordovician|||||||
13259|Mountain Creek Conglomerate|42304|6|Mentioned|p5|||Variation of Mountain Creek Conglomerate Member.||||||
13259|Mountain Creek Conglomerate|42500|5|Briefly described|p12|||||||||
13259|Mountain Creek Conglomerate|42620|1|Redefined|p45||Late Ordovician|Elevated to Formation status from member status.||||||22-APR-09
13259|Mountain Creek Conglomerate|43060|5|Briefly described|p37|||||||||
13259|Mountain Creek Conglomerate|43083|3|Fully described|p28, p35 Tb. 3, p46||Late Ordovician|Geological province: Hodgkinson Province. Mainly massive conglomerate. Of Fawckner (1981). Arenites.||||||31-JUL-20
13259|Mountain Creek Conglomerate|43213|5|Briefly described|p65|||Western margin of Hodgkinson Province. Basal limestone has a preliminary middle Ashgillian age. Volcanic clasts range from andesite to rhyolite, Zr-dated at 455 +/- 5 Ma (Bultitude et al., 1993).||||Correlated with Fork Lagoons beds.|Volcaniclastic conglomerate and arenite overlying a subordinate basal limestone.|
13259|Mountain Creek Conglomerate|43285|5|Briefly described|Map Legend||Late Ordovician|||||||
13259|Mountain Creek Conglomerate|43625|4|Described|p19,20|||Age: 455+/-5 Ma (SHRIMP)||||||19-APR-18
13259|Mountain Creek Conglomerate|60357|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Geological Province: Hodgkinson Province. Conglomerate, limestone, arenite.||||||
13259|Mountain Creek Conglomerate|60358|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Conglomeratic arenite, feldspathic arenite, conglomerate. Geological Province: Hodgkinson Province.||||||18-AUG-04
13259|Mountain Creek Conglomerate|60425|3|Fully described|p13, p18 Tb. 1, p20-21|Late Ordovician|Late Ordovician|Faulted against Mulgrave Fm.Thickness est'd to be in 100's of metres. Age: 455+/-5Ma (SHRIMP). Geol.prov: Hodgkinson Prov.Mainly pebble-boulder conglomerate with subordinate interbedded arenite; minor basal limestone; rich conodont fauna. Detailed lith.||||||07-FEB-11
13259|Mountain Creek Conglomerate|62371|5|Briefly described|p472 Fig.3|Ordovician|Ordovician|Mixed shallow marine sediments.||||||
13259|Mountain Creek Conglomerate|63140|5|Briefly described|p570, p572 Fig.3, p582, p583 Fig.13.|Late Ordovician|Late Ordovician|Western Hodgkinson Province. Product of arc-magmatism during a major eustatic episode; contains rare dacite clasts with SHRIMP crystallisation ages of 455 +/- 5 Ma.||||Overlies Mulgrave Formation unconformably.||
13259|Mountain Creek Conglomerate|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Hodgkinson Province. Mixed shallow marine sediments.||||||11-APR-07
13259|Mountain Creek Conglomerate|67848|5|Briefly described|p16.|||Western margin of Hodgkinson Province. Undated; possibly Ordovician. Comparable rock assemblage to the arc assemblage and Wairuna Formation of Broken River Province. Contains volcanic debris as well as limestone lenses, in part oolitic, of late Ordovician age.||||||
13259|Mountain Creek Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Hodgkinson Province. This unit, as well as Quadroy Conglomerate, Van Dyke Litharenite and Mulgrave Formation, are all mapped under the symbol, Om.||||||
13259|Mountain Creek Conglomerate|69030|5|Briefly described|p6|Silurian|Ordovician|Chillagoe Subprovince, Hodgkinson Province.|455 +/- 5 Ma (SHRIMP max. deposition age).|||||
13259|Mountain Creek Conglomerate|69079|6|Mentioned|p3-4|||Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|69592|5|Briefly described|p230-233, p241, p245,p255,p297,p301,p304|Late Ordovician|Late Ordovician|Chillagoe Subprovince, Hodgkinson Province. Crops out as discontinuous, N-trending lenses north of the Mitchell River, on the W edge of Hodgkinson Province. Thickness to ca.100m. Youngs to the east. Contains clasts lithologically identical to sandstones of Mulgrave Formation (both units referred to as Thomson Orogen strata). Contains mid-Ashgillian conodonts; also a clast dated at 455 +/- 5 Ma (SHRIMP U-Pb zircon: Domalga, 1997).|455-445 Ma.|||Is faulted against and structurally intercalated with Mulgrave Formation.|Mainly massive, very thick-bedded, clast-supported conglomerate; subordinate basal fossiliferous limestone beds to 30m thick, and fine- to medium-grained sandstone. Clast lithologies described.|
13259|Mountain Creek Conglomerate|70207|6|Mentioned|p1, p74, p94, p96||Late Ordovician|Thomson Orogen. Included in a group of units collectively aged as Ordovician-Silurian & Carboniferous?.||||||
13259|Mountain Creek Conglomerate|70345|6|Mentioned|p3|Carboniferous|Late Ordovician|||||||
13259|Mountain Creek Conglomerate|70673|6|Mentioned|p7|||Age (range) given as "Late Ordovician & Carboniferous?[sic]".||||||
13259|Mountain Creek Conglomerate|71031|5|Briefly described|p4-p5, p70-p72|Upper Ordovician|Upper Ordovician|Thomson Orogen, Hodgkinson Province.||||||
13259|Mountain Creek Conglomerate|72983|6|Mentioned|p15|Carboniferous?|Ordovician|||||||
13259|Mountain Creek Conglomerate|73595|6|Mentioned|p1134|||Hodgkinson Province, Mossman Orogen.||||||
13271|Mountain View Quartz Diorite|23422|5|Briefly described|p219 Table 6.12|||||||||
13271|Mountain View Quartz Diorite|23513|5|Briefly described|Map legend||Devonian|Palaeozoic Intrusive No. 453. I-Type.||||||
13271|Mountain View Quartz Diorite|42750|6|Mentioned|p46|||refers to Hartley & others (1989).||||||
13271|Mountain View Quartz Diorite|43259|4|Described|Appendix 1,p48.||Ordovician|Devonian?, possibly Ordovician.||||||12-FEB-09
13271|Mountain View Quartz Diorite|62521|5|Briefly described|p18|Late Carboniferous||Intrudes Deane Granodiorite. Geological Province: Ravenswood Batholith.||||||21-DEC-07
13363|Mulgildie Coal Measures|12597|5|Briefly described|p492 Tb.1, p498, p501, p506|Callovian|Callovian|Mulgildie Basin. 150m thick. Coal deposits briefly described.||||Equivalent to Walloon Subgroup and Walloon Coal Measures.|Sandstone, siltstone, shale and coal.|
13363|Mulgildie Coal Measures|24225|5|Briefly described|p381|Middle Jurassic|Middle Jurassic|||||||
13363|Mulgildie Coal Measures|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|Carboneous mudstone, labile to quartzose sandstone, minor coal.||||||
13363|Mulgildie Coal Measures|24615|5|Briefly described|CD|Jurassic|Jurassic|[Jm].  Carbonaceous mudstone, labile to quartzose sandstone, minor coal.||||||
13363|Mulgildie Coal Measures|29393|6|Mentioned|p11|||Jurassic.||||||
13363|Mulgildie Coal Measures|30451|3|Fully described|p75|||See also P76||||||
13363|Mulgildie Coal Measures|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
13363|Mulgildie Coal Measures|31086|6|Mentioned|p35|||Fossil flora||||||
13363|Mulgildie Coal Measures|31117|5|Briefly described|p379|||Mid Jurassic. Lithology.||||||19-AUG-08
13363|Mulgildie Coal Measures|32354|6|Mentioned|p325|||||||||
13363|Mulgildie Coal Measures|33774|3|Fully described|p53|||||||||
13363|Mulgildie Coal Measures|35935|6|Mentioned|p506|||||||||
13363|Mulgildie Coal Measures|36243|6|Mentioned|Table 10A|||||||||
13363|Mulgildie Coal Measures|36333|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
13363|Mulgildie Coal Measures|37065|6|Mentioned|p39|||||||||
13363|Mulgildie Coal Measures|37119|4|Described|p318|||||||||
13363|Mulgildie Coal Measures|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
13363|Mulgildie Coal Measures|39445|5|Briefly described|Table 10|||||||||
13363|Mulgildie Coal Measures|39632|6|Mentioned|p209|||||||||
13363|Mulgildie Coal Measures|39943|6|Mentioned|Table 12A|||||||||
13363|Mulgildie Coal Measures|42648|5|Briefly described|p42|||||||||
13363|Mulgildie Coal Measures|43008|5|Briefly described|map legend|||||||||
13363|Mulgildie Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
13363|Mulgildie Coal Measures|43983|14|Not recorded|p2,Fig.1|||||||||
13363|Mulgildie Coal Measures|43998|4|Described|p14,17,map||Middle Jurassic|||||||
13363|Mulgildie Coal Measures|44028|14|Not recorded|Fig.7,2,p509,513-514||Jurassic|Originally "Mulgeldie Coal Measures". See Strat Table.||||||
13363|Mulgildie Coal Measures|44029|14|Not recorded|p153,154,172||Middle Jurassic|||||||
13363|Mulgildie Coal Measures|44091|14|Not recorded|p58||Jurassic|Equivalent of Walloon Coal Measures.||||||
13363|Mulgildie Coal Measures|44104|14|Not recorded|p280|||||||||
13363|Mulgildie Coal Measures|44360|14|Not recorded|p36||Jurassic|||||||
13363|Mulgildie Coal Measures|44369|14|Not recorded|p170-171|||||||||
13363|Mulgildie Coal Measures|44379|14|Not recorded|p21,24||Jurassic|||||||
13363|Mulgildie Coal Measures|45168|6|Mentioned|p10|||||||||
13363|Mulgildie Coal Measures|60282|5|Briefly described|p11|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
13363|Mulgildie Coal Measures|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|Carbonaceous mudstone, labile to quartzose sandstone, minor coal.||||||
13363|Mulgildie Coal Measures|63748|6|Mentioned|p23|||Geological province: Mulgildie Basin. Equivalent of Walloon Coal measures in the Clarence-Moreton Basin.||||||07-FEB-11
13363|Mulgildie Coal Measures|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Overlies Hutton Sandstone. Carbonaceous mudstone, labile to quartzose sandstone, minor coal.||||||19-AUG-08
13363|Mulgildie Coal Measures|64665|5|Briefly described|p62.|Cretaceous|Cretaceous|Mulgildie Basin. Equivalent to Walloon Subgroup coals in the Surat Basin. Hosts hard, perhydrous, high ash coal seams; high volatile bituminous.||||||
13363|Mulgildie Coal Measures|65096|6|Mentioned|p368|||||||Equivalent of the Walloon Coal Measures.||
13363|Mulgildie Coal Measures|65388|3|Fully described|p214-215, 213|Jurassic.|Jurassic|First described by Reid (1927) and later by Cameron (1960), Dear & others (1971) and Whitaker & others (1974). Occupy the axial region of the synclinal Mulgildie basin and extend from near Monto to Kapaldo; forming a belt up to 7km wide to 350m thick. Conformably overlie the Hutton Sandstone. Overlain by unnamed freshwater Tertiary sediments. Correlated with Walloon Coal Measures on stratigraphic and lithological grounds. Sandstone, siltstone and mudstone.||||||
13363|Mulgildie Coal Measures|67402|5|Briefly described|p252, p253|Callovian|Callovian|Mulgildie Basin. 150 to 200m thick. Deposited in coal swamps or fluvial systems.||||Equivalent to the Walloon Subgroup.|Coarse-grained sandstone with granule conglomerate at the top grading into micaceous and carbonaceous mudstones and the base. Numerous coal seams occur throughout.|
13363|Mulgildie Coal Measures|68008|4|Described|p3, p188, p238, p240-243, p395,p485,p493|Middle Jurassic|Middle Jurassic|Originally the Mulgeldie [sic] Coal Measures of Reid (1927) from water bore records; he mapped their outcrop over 20 x 4 km along the axis of the Mulgildie Basin. Recessive; poor outcrop. Probably c.150m thick. Age from plant fossils. The coal is sub-bituminous and non-coking, suitable for power generation.||||Gradationally overlies Hutton Sandstone. Faulted against and/or unconformably overlies Cynthia beds. Correlated with Walloon Coal Measures, lower Injune Creek beds, upper part of Tiaro Coal Measures.|Interbedded sandstone, siltstone and shale, with a number of lenticular coal seams. Lithological descriptions by various authors are discussed.|
13363|Mulgildie Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Clarence-Moreton and Surat Basins. This unit, as well as the Injune Creek Group and the Walloon Coal Measures, are all mapped under the symbol, Ji.||||||
13363|Mulgildie Coal Measures|68679|6|Mentioned|p312-313, p338, p472|Jurassic|Jurassic|Northern New England Orogen.||||||
13363|Mulgildie Coal Measures|69594|5|Briefly described|p539|Jurassic|Jurassic|Dear et al. (1979). The name applies to the rock succession from Precipice Sandstone to Walloon Coal Measures, as they occur in the Mulgildie Basin. Contains potentially economic deposits. Up to 660m thick.||||||
13363|Mulgildie Coal Measures|72297|5|Briefly described|p700|Jurassic|Jurassic|Mulgildie Basin. Part of a 400m thick sequence. Potentially amenable to open-cut mining.||||Correlative of Walloon Coal Measures.|Contains several banded seams of perhydrous coal, high in volatiles, low sulfur and relatively low HGI.|
13363|Mulgildie Coal Measures|72298|6|Mentioned|p796|||A source of groundwater in the Monto area.||||||
13380|Mullaman beds|23374|5|Briefly described|p25|Cenomanian|Aptian|Subdivided into Walker River and Yirrkala Formations in eastern Arnhem Land.||||||
13380|Mullaman beds|23425|5|Briefly described|p381|||||||||
13380|Mullaman beds|24050|5|Briefly described|p53|Albian|Neocomian|Previuosly the Mullaman Group.||||||
13380|Mullaman beds|31268|6|Mentioned|Table 1|||||||||
13380|Mullaman beds|36335|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|36439|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|36442|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|38291|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late and/or Early Cretaceous||||||
13380|Mullaman beds|38348|6|Mentioned|p25|||||||||
13380|Mullaman beds|38350|6|Mentioned|p22|||||||||
13380|Mullaman beds|38584|4|Described|p21|||||||||
13380|Mullaman beds|39422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Clayey sandstone, claystone, conglomerate.  Unconformably overlies rocks of the South Nicholson Group, and over the Camooweal Dolomite.||||||10-MAR-05
13380|Mullaman beds|39497|6|Mentioned|p16|||||||||
13380|Mullaman beds|39523|6|Mentioned|p96|||||||||
13380|Mullaman beds|39797|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
13380|Mullaman beds|39925|6|Mentioned|Fig.2|||||||||
13380|Mullaman beds|41268|6|Mentioned|Fig.15|||||||||
13380|Mullaman beds|41406|6|Mentioned|Map legend|Early Cretaceous||||||||
13380|Mullaman beds|42821|5|Briefly described|p66|||||||||
13380|Mullaman beds|43630|6|Mentioned|p8||Mesozoic|Old name no longer in use||||||
13380|Mullaman beds|44112|6|Mentioned|p79,82|||Subdivided into newly defined 'Walker River Formation' and 'Yirrkala Formation' based on work by Krassey (1994a,b)||||||
13380|Mullaman beds|44922|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, claystone, siltstone, minor conglomerate.||||||01-JUL-04
13380|Mullaman beds|45148|3|Fully described|p20|||Briefly described p5.||||||07-OCT-22
13380|Mullaman beds|47083|6|Mentioned|p19|||||||||
13380|Mullaman beds|50600|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Quartz sandstone and siltstone.||||||
13380|Mullaman beds|61155|5|Briefly described|p16|||Age is pre-Cainozoic. Geological region: South Alligator Valley, East Arnhem Land and Barkly Tableland.||||||
13380|Mullaman beds|65239|5|Briefly described|p3 Fig. 4|Cretaceous|Cretaceous|Geological province: Wiso Basin. Fluvial deposits.||||||
13380|Mullaman beds|65345|5|Briefly described|p7 Fig.6. |Cretaceous|Cretaceous|Wiso Basin. Fluvial deposits.||||||
13380|Mullaman beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p106|Early Cretaceous|Late Jurassic|Eromanga/Carpentaria Basins.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|67564|5|Briefly described|p51.|Middle Aptian|Middle Aptian|Defined by Skwarko (1966). Correlated with parts of the Petrel and Darwin Formations; now defunct. Earliest marine sediments of the Dunmarra Basin coastal belt. Forms the Bulademo Tableland.||||||
13380|Mullaman beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Carpentaria Basin. This unit is mapped with Lees Sandstone, and unnamed sedimentary units, under the symbol, JKm.||||||
13380|Mullaman beds|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area; mapped as one unit with Lees Sandstone and unnamed sediments.||||||
13380|Mullaman beds|69594|5|Briefly described|p521-522|Early Cretaceous|Early Cretaceous|Western Gulf Sub-basin (NT), Carpentaria Basin. Occurs on WESTMORELAND and LAWN HILL 250K sheets. In NT, where the type region is located, this name has been replaced by Walker River Formation and Yirrkala Formation (Krassay, 1994; after Skwarko, 1966), "thus leaving the Mullaman beds as an anachronism" [?but not yet obsolete]. Age is poorly constrained: possible equivalent units mentioned.|||||Thin, mesa-forming sandstones with overlying siltstone or claystone.|
13380|Mullaman beds|69673|6|Mentioned|p202|||Discontinued name.||||||
13380|Mullaman beds|71369|5|Briefly described|p45|Early Cretaceous|Late Jurassic|Swarko (1966). Scattered remnants in far NW Queensland and adjacent NT. Mainly flat-lying. Thickness varies from a few metres to 15-20m. Rocks at higher elevations invariably occur in a zone of deep weathering, with lateritic profiles developed in the claystones.|||||Basal sandstone and granule conglomerate, commonly ferruginous, overlain by claystone.|
13380|Mullaman beds|72414|4|Described|map sheet|Early Cretaceous|Late Jurassic|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||Underlain unconformably nu Camooweal Dolomite.|Quartz sandstone and conglomerate, sandy claystone and siltstone.|
13380|Mullaman beds|72415|4|Described|mapsheet|Early Cretaceous|Late Jurassic|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||||Underlain unconformably nu Camooweal Dolomite.|Quartz sandstone and conglomerate, sandy claystone and siltstone.|
13380|Mullaman beds|72421|4|Described|mapsheet|Early Cretaceous|Late Jurassic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|72422|4|Described|mapsheet|Early Cretaceous|Late Jurassic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Quartz sandstone and conglomerate, sandy claystone and siltstone|
13380|Mullaman beds|73137|6|Mentioned|p6|Early Cretaceous|Jurassic|||||||
13391|Mullera Formation|23393|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Group.||||||
13391|Mullera Formation|23937|5|Briefly described|p76 App. 1|||Of the South Nicholson Group.  Overlies Constance Sandstone.||||||18-APR-05
13391|Mullera Formation|24047|5|Briefly described|p27|||Of the South Nicholson Group.  Geological Province: South Nicholson Basin.||||||
13391|Mullera Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the South Nicholson Group.||||||
13391|Mullera Formation|26310|2|Defined|p1, 3, 4, 8, 10, Table 1|Proterozoic|Proterozoic|Maximum Thickness: 8,000 feet. Type section in text. Underlies Tidna Sandstone (conformably), Colless Volcanics (unconformably), Camooweal Dolomite (unconformably).  Overlies: Constance Sandstone (conformably). Siltstone, sandstone, shale, ironstone.||||||13-NOV-06
13391|Mullera Formation|31420|6|Mentioned|p216|||||||||
13391|Mullera Formation|32660|5|Briefly described|Table 5|||||||||
13391|Mullera Formation|36003|6|Mentioned|p1029|||See also Fig.8.||||||
13391|Mullera Formation|36012|6|Mentioned|p26|||||||||
13391|Mullera Formation|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
13391|Mullera Formation|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||13-NOV-06
13391|Mullera Formation|37462|6|Mentioned|p263|||||||||
13391|Mullera Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13391|Mullera Formation|38348|6|Mentioned|p24|||||||||
13391|Mullera Formation|38584|4|Described|p20|||||||||
13391|Mullera Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the South Nicholson Group.  Contains the Middle Creek Sandstone Member.  Siltstone, shales, sandstone and ironstone.  Unconformably overlain by the Mullaman beds; conformably overlies Constance Sandstone.||||||22-JUL-13
13391|Mullera Formation|39445|5|Briefly described|Table 3|||300 million tonnes iron ore. Age: 1135 Ma - see p55.||||||13-NOV-06
13391|Mullera Formation|39497|4|Described|p15|||||||||
13391|Mullera Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13391|Mullera Formation|39925|6|Mentioned|Fig.2|||||||||
13391|Mullera Formation|41721|4|Described|p29|||||||||
13391|Mullera Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
13391|Mullera Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|of South Nicholson Group. Of "Mid Proterozoic" age.||||||
13391|Mullera Formation|44091|14|Not recorded|p11||Neoproterozoic|||||||
13391|Mullera Formation|44271|2|Defined|p40,41,57,60,62|||Conformably overlies Constance Sandstone. Overlain by Camooweal Dolomite.||||||
13391|Mullera Formation|44274|2|Defined|Tb.2,p9,10,15,16,map|||||||||
13391|Mullera Formation|44275|14|Not recorded|Map Legend|||||||||
13391|Mullera Formation|44281|14|Not recorded|Map Legend||Neoproterozoic|||||||
13391|Mullera Formation|44290|2|Defined|p439||Paleoproterozoic|||||||07-NOV-08
13391|Mullera Formation|44301|14|Not recorded|p.7|||Occurs on MT DRUMMOND sheet. (E53-12).||||||13-NOV-06
13391|Mullera Formation|44305|14|Not recorded|p.15|||(E53-8). opp.6,18.||||||
13391|Mullera Formation|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
13391|Mullera Formation|44441|14|Not recorded|p.7||Neoproterozoic|Overlain by Mittiebah Sandstone in E53-12 (Mt.Drummond). Upper Proterozoic.||||||13-NOV-06
13391|Mullera Formation|44482|14|Not recorded|p.5,7,9,opp.p.6, map|||(E53-12). See also p.10,13,15,16, for more details.||||||
13391|Mullera Formation|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
13391|Mullera Formation|44521|14|Not recorded|p8||Neoproterozoic|||||||
13391|Mullera Formation|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
13391|Mullera Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of South Nicholson Group.  Includes the Train Range Ironstone and Middle Creek Sandstone Members.||||||01-JUL-04
13391|Mullera Formation|44989|2|Defined|p.119,120|||Tb.II. (E53-4,8). On many pages.||||||
13391|Mullera Formation|45032|14|Not recorded|p7||Adelaidean|||||||
13391|Mullera Formation|45052|3|Fully described|p71|||Adelaidean||||||
13391|Mullera Formation|45079|6|Mentioned|p75|||Diagram on p75. Upper Proterozoic age.||||||13-NOV-06
13391|Mullera Formation|45166|5|Briefly described|p33|||||||||
13391|Mullera Formation|45287|14|Not recorded|p.223,226,229,231||Neoproterozoic|||||||
13391|Mullera Formation|48894|6|Mentioned|p24|||Age||||||
13391|Mullera Formation|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Accident Subgroup. Green, grey and reddish brown to maroon, micaceous, locally ferruginous siltstone, shale and fine grained, lithic to quartzose sandstone.||||||
13391|Mullera Formation|64443|5|Briefly described|p3, p4, p6, p29|Calymmian|Calymmian|||Of the Accident Subgroup.||Possibly unconformably overlies Mittiebah Sandstone.|Typically comprises fine-coarse, quartzose to sublithic sandstone with minor interbeds of conglomerate and siltstone, medium-very thick bedding with scattered-entrained quartz granules and pebbles.|14-MAY-14
13391|Mullera Formation|65337|3|Fully described|p9 Fig.5, p38 Table 5, pp57-60.|Mesoproterozoic|Mesoproterozoic|Northwest MOUNT DRUMMOND area. Thickness over 1100 m. Distribution now substantially less than previous maps as many outcrops have been reassigned. Contains shale rich in hydrocarbons (TOC c.10%) with low thermal maturity.||Unit in Accident Subgroup.|Includes Middle Creek Sandstone Member.|Overlies Mittiebah and Constance Sandstones. Is overlain by Tidna Sandstone.|Green to maroon, micaceous, locally ferruginous siltstone, shale and fine-grained, lithic to quartzose sandstone; minor ironstone, organic-rich shale and medium-grained quartzose sandstone.|
13391|Mullera Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p39|Neoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. South Nicholson Basin.||South Nicholson Group.|||Siltstone, shale, some sandstone and ironstone.|
13391|Mullera Formation|67352|6|Mentioned|p12, p16|Calymmian|Calymmian|||Accident Subgroup||||
13391|Mullera Formation|67539|5|Briefly described|p14, p15 Fig.8|||Thin ironstones of the Boodjamulla Formation were previously mapped as the Mullera Formation.||Of the South Nicholson Group.|Includes Train Range Ironstone Member and Middle Creek Sandstone Member.|Overlain by the Tidna Formation. Underlain by the Constance Sandstone.||
13391|Mullera Formation|68020|6|Mentioned|p128|||||?Of South Nicholson Group||||
13391|Mullera Formation|68146|5|Briefly described|p196|||||Accident Subgroup.|Middle Creek Sandstone Member, Train Range Ironstone Member.|Conformably overlies Elizabeth Sandstone Member. Is overlain by Tidna Sandstone.||
13391|Mullera Formation|68575|6|Mentioned|p28|||South Nicholson Basin.||||Is overlain conformably and gradationally by Tidna Sandstone.||
13391|Mullera Formation|69434|4|Described|p19:2, 4-8|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Mapping of this unit by Smith and Roberts (1963) included rocks now assigned to the Crow Formation. Over 1100m thick (in NT); up to 1800m thick (in Qld). Very recessive. A variety of sedimentary structures are listed. Shallow-marine shelf deposits, partly above storm wave-base and partly below. Several ironstone intervals in Qld, grouped as the Train Range Ironstone Member, were explored for iron. Hosts several "Clinton-type" oolitic iron ore occurrences (described) in NT. Has mixed indications, mostly negative, for petroleum potential. A whole-rock (shale) Rb-Sr date of 1510 +/- 120 Ma (Plumb and Derrick, 1975) is considered unreliable due to possible inherited material.||Accident Subgroup.|Middle Creek Sandstone Member, Train Range Ironstone Member.|Conformably overlies Constance Sandstone. Is overlain conformably by Tidna Sandstone (in Qld).|Green or red-brown to maroon, micaceous, locally ferruginous siltstone, shale and lithic to quartzic fine sandstone; minor ironstone, organic-rich shale and medium quartzic sandstone. Characteristically thinly-bedded.|12-JUL-16
13391|Mullera Formation|69445|6|Mentioned|p30:17|||||||Is overlain by Colless Volcanics.||12-JUL-16
13391|Mullera Formation|69591|4|Described|p52, p54, p88, p98, p111|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Mainly deep marine, locally shallowing, deposits.||Uppermost Accident Subgroup.|Train Range Ironstone Member, Middle Creek Sandstone Member.|Overlies Elizabeth Sandstone. Is overlain by Yidna Sandstone.|Predominantly deeper marine shales and siltstone, punctuated by shallower sandstone and oolitic ironstone units.|
13391|Mullera Formation|69673|6|Mentioned|p56, p57|||Up to 1100m thick. Deposited in shallow marine shelf environment.||Accident Subgroup|||Micaceous, locally ferruginous siltstone, shale and lithic to quartzose sandstone, organic rich shale and quartzose sandstone.|
13391|Mullera Formation|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||South Nicholson Group.||Overlies Constance Sandstone. Is overlain by Mittiebah Sandstone.|Fine- to coarse-grained quartz sandstone; greywacke and siltstone, commonly rich in iron oxides.|
13391|Mullera Formation|70897|5|Briefly described|p41-42, Fig.1.7.6,8|Mesoproterozoic|Mesoproterozoic|Results of dating of six samples' detrital zircons are tabulated and graphed. The youngest result is assumed to be the maximum depositional age.|1492 +/- 4 Ma (maximum depositional age).|South Nicholson Group.|||Green to grey, carbonaceous siltstone and shale; pyritic grey shale; pale green tuffaceous clay.|
13391|Mullera Formation|70968|5|Briefly described|p131 Fig.118, p132|Ectasian|Ectasian|May correlate with the Maiwok Subgroup.||Accident Subgroup.||||
13391|Mullera Formation|71369|4|Described|p1, p4-6, p22-23, p36-44, p48, p50|Mesoproterozoic|Mesoproterozoic|Mapped by Carter and Opik (1961); defined by them in Carter et al. (1961). Revised by Carter and Zimmerman (1960) [sic], who named the Tidna Sandstone as a separate Formation rather than the uppermost Member of this unit. South Nicholson Basin. Occupies a series of structural basins. 1020-2460m thick. Lithologies, particularly the ironstones, described in great detail. Age is derived from U-Pb zircon.|1569 +/- 19 Ma (maximum depositional age)|Accident Subgroup.|Train Range Ironstone Member, Middle Creek Sandstone Member.|Conformably overlies Elizabeth Sandstone. Is overlain conformably and gradationally by Tidna Sandstone.|Dominantly mudstone (shale and siltstone), punctuated by sandstone, ferruginous sandstone and ironstone, and minor conglomerate.|20-FEB-18
13391|Mullera Formation|71592|5|Briefly described|Appendix A.|||South Nicholson Basin. Sixteen age determinations are given, for MDAs and provenance clusters.|1569+/- 38 Ma (MDA: U-Pb zircon SHRIMP)||||Siltstone, shale.|
13391|Mullera Formation|71779|5|Briefly described|p23, p24, 26 p27|||South Nicholson Basin. Probably equivalent to the Velkerri Formation.||||||24-SEP-18
13391|Mullera Formation|72297|5|Briefly described|p749|||South Nicholson Basin. Poor source material; organic material has mostly reached an advanced stage of thermal maturity.|||||Includes shales.|
13391|Mullera Formation|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member and Train Range Ironstone Member.||Siltstone, shale, sandstone and ironstone.|
13391|Mullera Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|
13391|Mullera Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|
13391|Mullera Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series. Various additional lithologies are provided.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|10-DEC-19
13391|Mullera Formation|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series. Lithology of numerous other outcrops provided.||Unit of Accident Subgroup.|Includes Middle Creek Sandstone Member, Train Range Sandstone Member.||Siltstone, shale, sandstone and ironstone|18-MAR-20
13391|Mullera Formation|72526|5|Briefly described|p8 Fig.1.3, p33, p40, p46, p56|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin. Assumed to conformably overlie Mittiebah Sandstone but contact not exposed.||Accident Subgroup|Probably includes  Middle Creek Sandstone Member, Train Range Ironstone [Member].|Conformably overlies Constance Sandstone. Overlies Mittiebah Sandstone.||
13391|Mullera Formation|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|South Nicholson Group.||Accident Subgroup|Includes Middle Creek Sandstone Member.|Overlies Mittiebah Sandstone and Constance Sandstone.|Includes sandstone.|
13391|Mullera Formation|72912|4|Described|p5 Fig.3, p23, p27-30, p32, p34.|Mesoproterozoic|Mesoproterozoic|Located in the west, central and east part of the South Nicholson Basin. This unit is considered to have good gas potential. See also p33 Fig.12, p34, p35 Fig.13, p37 Fig.14, p45.||Accident Subgroup|Middle Creek Sandstone Member, Train Range Ironstone Member|Overlies Mittiebah Sandstone, Constance Sandstone, underlies Tidna Sandstone.|Includes siltstone.|
13391|Mullera Formation|72913|5|Briefly described|p4, p7 Fig.2, p8, p9 Tb.1, p15, 16, 26|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern parts of the South Nicholson Basin. Mineral composition boxplots reveal dominant quartz, muscovite and kaolinite components. Identified in Amoco DDH 83-3 well.||Accident Subgroup|Middle Creek Sandstone Member, Train Range Ironstone.|Partially overlies Mittebah Sandstone, Bowthorn Member and Constance Sandstone and underlies Tidna Sandstone.|Includes siltstone, ironstone, sandstone.|
13391|Mullera Formation|72919|5|Briefly described|p5, p56-57, p70|Mesoproterozoic|Mesoproterozoic|Contact with underlying Mittiebah Sandstone is inferred to be conformably but is not exposed. Withnall and Hutton (2013) suggested the unit may be present in Morstone 1 as the portion containing glauconitic sandstones and finer units.||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone Member|Underlain by Elizabeth Sandstone, Mittiebah Sandstone and Constance Sandstone, including Schultz Sandstone Member. Overlain by Tidna Sandstone and Bukalara Sandstone (unconformably).||
13391|Mullera Formation|72967|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group||||
13391|Mullera Formation|73042|5|Briefly described|p4, p6, p9-11|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. Maximum thickness: >1100m (Ahmad and Munson, 2013). Previous maximum depositional ages include 1550 +/- 51 Ma (Yang, 2019) and between ca 1750 and 1570 Ma elsewhere (Jones et al., 2018 and references therein). Present day hydrogen index suggests the unit has no present-day potential for hydrocarbon generation at the sampled locality (Jarrett et al., 2019). Re-Os sample 2777644 is tentatively interpreted as belonging to the Mullera Formation (?Mullera Formation), although a geologically permissible regression age could not be obtained. (Relationship between Mullera Formation and its possible constituents (Middle Creek Sandstone Member, Train Range Ironstone) is not clear in Fig.1.2.)||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone.|Underlain by Constance Sandstone conformably and Mittiebah Sandstone. Partly overlain by Tidna Sandstone.|Siltstone, shale, sandstone, with minor ironstone.|
13391|Mullera Formation|73083|6|Mentioned|p34-35|Mesoproterozoic|Mesoproterozoic|Has numerous iron-bearing rock types, although mapped exposures have a bland, featureless, non-layered magnetic character.||||Overlain by Mittiebah Sandstone.|Includes siltstone (locally ferruginous), glauconitic sandstone with hematite 'dustings', ferruginous sandstone, ferruginous siltstone, and ironstone.|
13391|Mullera Formation|73098|6|Mentioned|p4, p7, p17|||South Nicholson Basin. Organic petrolography performed on four samples from the NTGS 00/1 well. Laminated component is characterised by alternations of bitumen-lean and bitumen-rich layers. [See report for bitumen/maceral description].|||||Includes grey to black shale and laminated brown to dark grey shale.|
13391|Mullera Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Aquitard with potential shale gas/oil play.||Accident Subgroup, South Nicholson Group|Middle Creek Sandstone Member, Train Range Ironstone|Underlain by Elizabeth Sandstone. Overlain by Tidna Sandstone.||
13438|Mundic Igneous Complex|22630|5|Briefly described|p39|||||||||
13438|Mundic Igneous Complex|22844|6|Mentioned|p39|||||||||
13438|Mundic Igneous Complex|23049|3|Fully described|p73|Late Permian|Late Permian|||||||
13438|Mundic Igneous Complex|23422|5|Briefly described|p219 Table 6.12|||Of Mundic Suite.||||||
13438|Mundic Igneous Complex|23505|5|Briefly described|Map legend|Permian|Late Carboniferous|||||||
13438|Mundic Igneous Complex|23508|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
13438|Mundic Igneous Complex|30151|4|Described|Table 2|||Upper Permian age. See also Table 5.||||||
13438|Mundic Igneous Complex|30914|6|Mentioned|Map legend|Permian|Permian|||||||
13438|Mundic Igneous Complex|31813|6|Mentioned|Table 2|||U.Permian||||||
13438|Mundic Igneous Complex|32553|4|Described|p58|||||||||
13438|Mundic Igneous Complex|33644|6|Mentioned|Map legend|Late Permian|Late Permian|Prob.Upper Permian||||||
13438|Mundic Igneous Complex|33648|4|Described|p11|||Upper Permian?||||||
13438|Mundic Igneous Complex|34408|6|Mentioned|p185|||On Table||||||
13438|Mundic Igneous Complex|34409|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
13438|Mundic Igneous Complex|36472|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
13438|Mundic Igneous Complex|37613|6|Mentioned|Fig.3|||||||||
13438|Mundic Igneous Complex|37764|6|Mentioned|Table 1|||||||||
13438|Mundic Igneous Complex|39445|5|Briefly described|Table 12|||||||||
13438|Mundic Igneous Complex|39734|6|Mentioned|p21|||||||||
13438|Mundic Igneous Complex|40958|6|Mentioned|Table 1|||||||||
13438|Mundic Igneous Complex|41272|5|Briefly described|M 1of1 K07|||||||||
13438|Mundic Igneous Complex|43259|4|Described|Appendix 1,p31.||Late Permian|||||||
13438|Mundic Igneous Complex|45151|5|Briefly described|Table 10|||||||||
13438|Mundic Igneous Complex|48903|3|Fully described|p25|||U.Perm. ? See also Table 1.||||||
13438|Mundic Igneous Complex|48914|4|Described|p47|||Se also PP48-50. U.Perm.||||||
13438|Mundic Igneous Complex|69593|5|Briefly described|p494, p513|Permian|Permian|Paluma Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|~285-265 Ma (Rienks, 1997).|Mundic Suite.|||Biotite and hornblende-biotite granite and granodiorite; minor diorite/gabbro, andesite and rhyolite. I-type.|
13448|Mundubbera Sandstone|31586|6|Mentioned|p6|||Correlation of coral horizons||||||
13448|Mundubbera Sandstone|31587|6|Mentioned|p60|||Lithostrotion distribution||||||
13448|Mundubbera Sandstone|32388|6|Mentioned|Fig.1|||||||||
13448|Mundubbera Sandstone|32866|6|Mentioned|p22|||Fossil content||||||
13448|Mundubbera Sandstone|32867|6|Mentioned|p46|||||||||
13448|Mundubbera Sandstone|34085|6|Mentioned|Cor.chart|||Visean||||||
13448|Mundubbera Sandstone|42547|5|Briefly described|p52|||||||||
13448|Mundubbera Sandstone|44360|14|Not recorded|p13,30-32||Early Carboniferous|||||||
13448|Mundubbera Sandstone|45097|6|Mentioned|Fig.|||Correlation chart||||||
13448|Mundubbera Sandstone|46803|6|Mentioned|Fig. 4|||||||||
13449|Munduran Creek Member|39493|2|Defined|p96|late Eocene|middle Eocene|Mid to late Eocene||||||
13449|Munduran Creek Member|40116|6|Mentioned|p37|||||||||
13449|Munduran Creek Member|41927|5|Briefly described|p64|||||||||
13449|Munduran Creek Member|42021|6|Mentioned|Fig.1 p320|||||||||
13449|Munduran Creek Member|71092|6|Mentioned|p232|Eocene|Eocene|||Rundle Formation.||||
13449|Munduran Creek Member|72297|5|Briefly described|p753 Fig.10.45|||Narrows Graben.||Rundle Formation.||||
13468|Mungerebar Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 30m.||||||
13468|Mungerebar Limestone|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
13468|Mungerebar Limestone|31286|4|Described|p57|||Early Cambrian. Mindyallan Stage.||||||
13468|Mungerebar Limestone|33111|6|Mentioned|Fig.15|||||||||
13468|Mungerebar Limestone|35054|6|Mentioned|Table 23|||||||||
13468|Mungerebar Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
13468|Mungerebar Limestone|35139|4|Described|Table.2|||||||||
13468|Mungerebar Limestone|37275|6|Mentioned|p291|||||||||
13468|Mungerebar Limestone|37572|4|Described|p161|||See also p165 and Fig.8.||||||13-NOV-06
13468|Mungerebar Limestone|38446|6|Mentioned|Table 23|||||||||
13468|Mungerebar Limestone|38532|4|Described|Fig.1|||||||||
13468|Mungerebar Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||13-NOV-06
13468|Mungerebar Limestone|39690|6|Mentioned|p88|||||||||
13468|Mungerebar Limestone|40038|6|Mentioned|p248|||||||||
13468|Mungerebar Limestone|41003|5|Briefly described|p196|||||||||
13468|Mungerebar Limestone|41810|6|Mentioned|p112|||||||||
13468|Mungerebar Limestone|42139|6|Mentioned|Fig.19 P74|||||||||
13468|Mungerebar Limestone|42994|6|Mentioned|p8|||||||||
13468|Mungerebar Limestone|44205|4|Described|p46,47|||||||||
13468|Mungerebar Limestone|44211|2|Defined|p91,95-96,100-104|||Rests on Steamboat Sandstone. Marks boundary against overlying Georgina Limestone.||||||
13468|Mungerebar Limestone|44309|2|Defined|Tb.1,p7,8-11,17|||Disconformably underlies Ninmaroo Formation.||||||
13468|Mungerebar Limestone|44326|14|Not recorded|Map Legend|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|44543|2|Defined|p32,36|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|44719|14|Not recorded|p143|||Lowermost Upper Cambrian. Conodonts present.||||||13-NOV-06
13468|Mungerebar Limestone|44920|14|Not recorded|Map Legend, Sheet 4|Late Cambrian|Middle Cambrian|||||||
13468|Mungerebar Limestone|45002|14|Not recorded|p23,24,43,72|||Late Cambrian fossils.||||||
13468|Mungerebar Limestone|45012|14|Not recorded|p84-86,92-107,111-15||Late Cambrian|p145-149,205-278,282-296,326-37,343-44,263-372,381-2. Mindyallan fauna.||||||
13468|Mungerebar Limestone|45052|3|Fully described|p102|||M.Camb. See also p33.||||||13-NOV-06
13468|Mungerebar Limestone|45053|6|Mentioned|p12|||||||||
13468|Mungerebar Limestone|45079|6|Mentioned|p36|||Cambrian age. Lithology||||||
13468|Mungerebar Limestone|45115|6|Mentioned|p6|||||||||
13468|Mungerebar Limestone|45130|6|Mentioned|p61|||||||||
13468|Mungerebar Limestone|46958|6|Mentioned|Fig.2|||||||||
13468|Mungerebar Limestone|48906|14|Not recorded|App.D.|||||||||
13468|Mungerebar Limestone|48971|6|Mentioned|p10|||See also p30.||||||13-NOV-06
13468|Mungerebar Limestone|60122|6|Mentioned|p18|||Conformably overlies Steamboat Sandstone.||||||
13468|Mungerebar Limestone|62790|6|Mentioned|p208, 217|Middle Cambrian|Middle Cambrian|Eastern Georgina Basin. Contains the comptalutid Aristaluta spicata Opik, 1967, in its lower (late Boomerangian) part. Also contains the svealutid Anabarochilina chummyensis (Hinz-Schallreuter, 1993c), the only known Mindyallan bradoriid.||||||28-MAR-12
13468|Mungerebar Limestone|62791|6|Mentioned|p233, p236, p239|Late Cambrian|Middle Cambrian|Source of Type species of Picnotreta debilis and Stilpnotreta magna both Henderson & MacKinnon 1981 (Mindyallan Stage).||||||04-DEC-12
13468|Mungerebar Limestone|64068|3|Fully described|p69, p65, 67, 69, 73|Late Cambrian|Middle Cambrian|Diverse fossil fauna. Correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Selwyn Range Limestone, Cleland Sandstone. Trilobites indicate late Middle Cambrian (Boomerangian) Lejopyge laevigata Zone to early Late Cambrian (Mindyallan) Glyptagnostus stolidotus Zone (Shergold et al 1985, Shergold 1997)||Of Narpa Group.||Laterally interdigitates with and conformably overlies Steamboat Sandstone. Is overlain by Georgina Limestone conformably (Opik 1960) or Ninmaroo Formation disconformably.|Quartzic and ooid grainstone, dolomitic limestone, chert; dolostone and sandstone interbeds toward base.|21-MAR-16
13468|Mungerebar Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group|||Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
13468|Mungerebar Limestone|69443|5|Briefly described|p28:16, 26|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Is overlain disconformably by Ninmaroo Formation.||12-JUL-16
13468|Mungerebar Limestone|69573|6|Mentioned|p659, 661, 669|||Georgina Basin.||||||
13468|Mungerebar Limestone|69591|5|Briefly described|p87, p91, p93, p96|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. Appears as Mungereebar Limestone on p87. Up to 30m thick. Lithologically very similar to Quita Formation. Trilobite and conodont faunas indicate Lejopyge laevigata Zone to Mindyallan.||||Transitionally overlies and interfingers with Steamboat Sandstone. Is overlain unconformably/disconformably by Ninmaroo Formation.|Thin-bedded limestone with thin chert layers and nodules; upper boundary is marked by a fine-grained dolomite.|
13468|Mungerebar Limestone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Steamboat Sandstone. Is overlain by Georgina Limestone.|Limestone.|
13468|Mungerebar Limestone|72358|5|Briefly described|p125|||Of Georgina Basin. Includes G. stolidotus zone.||||Overlain by Georgina Limestone.||
13468|Mungerebar Limestone|72516|6|Mentioned|p93-94|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arrinthrunga Formation and the Eurowie Sandstone Member.||08-JUN-21
13473|Mungore Granite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
13473|Mungore Granite|40475|6|Mentioned|Table 2|||||||||
13473|Mungore Granite|41738|6|Mentioned|p169|||||||||
13473|Mungore Granite|41778|6|Mentioned|p370|||See also P377||||||
13473|Mungore Granite|43008|5|Briefly described|map legend|||||||||
13473|Mungore Granite|63821|4|Described|p32|Late Triassic|Late Triassic|Age: 212+/-4Ma (K-Ar biotite) and 219+/-4Ma (K-Ar biotite). Intrudes Gympie Group, Mount Marcella Volcanics and Johngboon Rhyolite. Comprises biotite granite, hornblende granite, granophyre and rhyolite.||||||07-FEB-11
13473|Mungore Granite|65452|5|Briefly described|p7 Tb.2, p37|Late Triassic|Late Triassic|Is "associated" with Aranbanga Volcanic Group. Is considered to represent extension-related magmatism. SHRIMP U-Pb zircon magmatic crystallisation age.|226.5 +/- 1.6 Ma (Cross, in prep.).||||Fine- to medium-grained, miarolitic, granophyric biotite-hornblende syenogranite.|
13473|Mungore Granite|67203|5|Briefly described|p3-4|Triassic|Triassic||226.5 +/- 1.6 Ma (Cross, unpublished).||||Fine- to medium-grained, miarolitic, granophyric biotite-hornblende syenogranite.|
13473|Mungore Granite|67874|5|Briefly described|p2-3, p7-10, p34, p49|Late Triassic|Late Triassic|Mungore Cauldron. Co-genetic with Johngboon Rhyolite. A sub-unit identified as Mungore Granite/g was dated: SHRIMP U-Pb zircon magmatic crystallisation age.|226.5 +/- 1.5 Ma (Cross et al., 2012).|||Intrudes Johngboon Rhyolite (Aranbanga Volcanic Group).|Includes biotite +/- hornblende, granophyric and miarolitic, leucocratic alkali feldspar granite.|
13473|Mungore Granite|68679|5|Briefly described|p428, p430, p436, p440|Late Triassic|Late Triassic|Northern New England Orogen. The only named one of the granites comprising the (upper magma chamber of the) Mungore Cauldron, the lithology, structure and age of which are described in detail on p430. Comagmatic with Aranbanga Volcanic Group.|226.5 +/- 1.6 Ma (SHRIMP: Cross et al., 2012).|||Intrudes Aranbanga Volcanic Group.|Biotite granite and a granophyre-rhyolite subunit. Mainly I-type; some A-type.|
13473|Mungore Granite|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|227+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
13473|Mungore Granite|72481|6|Mentioned|p429|||Topographically prominent occurrence southwest of Bundaberg.||||||
13473|Mungore Granite|73450|4|Described|p4, p25, p29-34|||Metaluminous I-type. Texturally heterogeneous. Forms extensively dissected, rugged, mountainous country. Stephens (1991) assigned the granites of the Mungore Complex (of Ellis, 1968) to the Mungore Granite and delineated 5 informal subdivisions. The main phase is truncated by Mount Walsh Granite. Has yielded various radioisotopic ages including K-Ar biotite ages of 212 Ma and 219 Ma (Webb and McDougall, 1967) and 'pooled' Rb-Sr ages of 226 +/- 16 Ma and 222 +/- 0.6 Ma (Ellis, 1968; Stephens, 1991). Interpreted as produced by ca 20 percent partial melting of (meta-) andesitic crust; genetically related to the Aranbanga Volcanic Group (Stephens, 1991).||||Intrudes Mount Marcella Volcanics and the Aranbanga Volcanic Group.|Medium-grained, slightly porphyritic biotite granite and (hornblende-) biotite granite, with some aplite and granophyre.|
13528|Murphy Metamorphics|22457|6|Mentioned|Fig29 P30|||||||||
13528|Murphy Metamorphics|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
13528|Murphy Metamorphics|22673|6|Mentioned|64|||Geological province: Mount Isa Basin. Overlain by Kalkadoon Granite, Leichardt Volcanics||||||13-NOV-06
13528|Murphy Metamorphics|23065|5|Briefly described|11|||||||||
13528|Murphy Metamorphics|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
13528|Murphy Metamorphics|23395|6|Mentioned|p390|||||||||
13528|Murphy Metamorphics|23405|5|Briefly described|p565|Statherian||Age: >1900Ma.||||||13-NOV-06
13528|Murphy Metamorphics|24419|6|Mentioned|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Murphy Province, Lawn Hill Subprovince (north); South Nicholson Basin.||||||07-NOV-08
13528|Murphy Metamorphics|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1850Ma.  Geological Province: McArthur Basin.  See also p22 Fig. 1.||||||07-NOV-08
13528|Murphy Metamorphics|31348|6|Mentioned|p343|||||||||
13528|Murphy Metamorphics|31421|6|Mentioned|p507|||||||||
13528|Murphy Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|32660|5|Briefly described|Table 2|||||||||
13528|Murphy Metamorphics|33900|6|Mentioned|p7|||Redate||||||
13528|Murphy Metamorphics|35114|6|Mentioned|Table.1|||||||||
13528|Murphy Metamorphics|35950|6|Mentioned|p304|||||||||
13528|Murphy Metamorphics|36439|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|36442|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13528|Murphy Metamorphics|37462|5|Briefly described|p234|||||||||
13528|Murphy Metamorphics|37565|6|Mentioned|Fig.5|||||||||
13528|Murphy Metamorphics|38066|6|Mentioned|Fig.9|||p53.||||||13-NOV-06
13528|Murphy Metamorphics|38584|4|Described|p4|||||||||
13528|Murphy Metamorphics|39338|6|Mentioned|p351|||||||||
13528|Murphy Metamorphics|39422|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Phyllite and quartz-sericite schist, quartzite, sandstone, siltstone, chert, ironstone (pyrite graphite schist below).  Unconformably overlain by Don Creek Sandstone (Carrara Range Group).  Probably Early Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|39497|4|Described|p5|||See also p17.||||||13-NOV-06
13528|Murphy Metamorphics|39685|6|Mentioned|Fig.1|||||||||
13528|Murphy Metamorphics|39925|6|Mentioned|Fig.9|||||||||
13528|Murphy Metamorphics|40489|6|Mentioned|p88|||||||||
13528|Murphy Metamorphics|40491|6|Mentioned|p79|||||||||
13528|Murphy Metamorphics|40840|6|Mentioned|Map legend|||||||||
13528|Murphy Metamorphics|41125|6|Mentioned|p35|||See also Fig.23||||||
13528|Murphy Metamorphics|41319|6|Mentioned|p195|||||||||
13528|Murphy Metamorphics|41381|6|Mentioned|p325|||||||||
13528|Murphy Metamorphics|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13528|Murphy Metamorphics|41721|3|Fully described|p2, p6|Paleoproterozoic|Paleoproterozoic|Overlain by Cliffdale Volcanics. Intruded by Nicholson Granite Complex. Geol.Prov: Murphy Inlier. Sequence of shale, siltstone, greywacke and volcanics, metamorphosed into greenschist facies quartz-albite-muscovite-biotite schist and gneiss.||||||07-NOV-08
13528|Murphy Metamorphics|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
13528|Murphy Metamorphics|41757|6|Mentioned|p207|||||||||
13528|Murphy Metamorphics|44305|14|Not recorded|p.6,8,9,10,15,17,18|||(E53-8). opp.6,18.||||||
13528|Murphy Metamorphics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|44482|14|Not recorded|p.6,9, opp. p.6, map|||(E53-12). See also p.13,14, for more details.||||||
13528|Murphy Metamorphics|44483|5|Briefly described|map legend||Paleoproterozoic|Defn. on Tech.File E/53-12. Lower Proterozoic.||||||07-NOV-08
13528|Murphy Metamorphics|45032|14|Not recorded|p9||Paleoproterozoic|Lower ?Proterozoic. Tb.1, Pl.1.||||||07-NOV-08
13528|Murphy Metamorphics|45052|4|Described|p69|||L.Prot. See also Table 9.||||||13-NOV-06
13528|Murphy Metamorphics|45140|6|Mentioned|p12-13|||McArthur Basin region.||||Possible correlative of Tanami Complex.||
13528|Murphy Metamorphics|45166|4|Described|p8|||||||||
13528|Murphy Metamorphics|45167|5|Briefly described|Fig.27|||||||||
13528|Murphy Metamorphics|46804|6|Mentioned|p153|||Stratigraphy||||||
13528|Murphy Metamorphics|49001|6|Mentioned|p1|||||||||
13528|Murphy Metamorphics|49018|6|Mentioned|p4|||||||||
13528|Murphy Metamorphics|50536|6|Mentioned|p3.2|||Intruded by Nicholson Suite.||||||
13528|Murphy Metamorphics|62659|5|Briefly described|Map Legend|Orosirian|Orosirian|Purple micaceous metasiltstone (phyllite), metagreywacke and quartz-mica schist with locally abundant quartz veins; minor metaquartzite, banded ironstone and calc-silicate rock.||||||
13528|Murphy Metamorphics|63866|5|Briefly described|p56||||||||Metasedimentary rocks, volcanics and migmatites.|
13528|Murphy Metamorphics|64575|6|Mentioned|p656|||Age: 1890Ma.||||||
13528|Murphy Metamorphics|65232|5|Briefly described|p9, p66, App. 2|||Unconformably underlies Cliffdale Volcanics. Intruded by  Nicholson Granite Complex. Deformed and metamorphosed succession of shale, siltstone, greywacke and volcanic rocks of Barramundi Orogeny at 1860-1845 Ma. U mineralisation. Geol Prov: Murphy Inlier.||||||09-FEB-10
13528|Murphy Metamorphics|65337|4|Described|p v, p6 Fig.3,  p10 Table 3. |Paleoproterozoic|Paleoproterozoic|Oldest exposed basement rocks in MOUNT DRUMMOND map area. Flysch sediments, metamorphosed and deformed during Barramundi Orogeny c.1870 Ma.|c.2100-1880 Ma.|||Is overlain by Connelly Volcanics, probably unconformably, and unconformably by Benmara and South Nicholson Groups.|Mainly turbiditic succession. Ferruginised outcrop and float of red-brown to purple or yellow, finely-laminated micaceous metasiltstone, metagreywacke and quartz-mica schist; minor metaquartzite and calc-silicate rock; local 5m thick horizon of BIF.|
13528|Murphy Metamorphics|65340|5|Briefly described|p7, p82.|Paleoproterozoic|Paleoproterozoic|Metasedimentary bedrock; multiple deformation and metamorphism to greenschist facies during the Barramundi Orogeny. Hosts abundant non-transported microdiamonds.|?2100 - 1845 Ma.||||Turbidites.|
13528|Murphy Metamorphics|66529|5|Briefly described|p20-21 |Paleoproterozoic|Paleoproterozoic|||||Unconformably overlain by the Cliffdale Volcanics.|Quartz-feldspar-mica schists and gneisses.|
13528|Murphy Metamorphics|67323|5|Briefly described|Mount Isa Block Time-Space Plot|Paleoproterozoic|Paleoproterozoic|See also p9, p29, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Camooweal - Murphy Domain, Mount Isa Inlier. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny.|1853 +/- 4 Ma (maximum depositional age).|||Intruded by Nicholson Granite. Overlain by Cliffdale Volcanics.||
13528|Murphy Metamorphics|68998|5|Briefly described|vi, p34-37|||Murphy Province.||||Is intruded by the Nicholson Granite Complex.||
13528|Murphy Metamorphics|69383|5|Briefly described|p38-43, 44|Paleoproterozoic|Paleoproterozoic|Murphy Inlier. LA-ICPMS U-Pb geochronology analyses. Max deposition age. Previously dated samples (Hanley 1996) were a little older: ~1870 Ma.|1853+/- 4 Ma|||Overlain by Westmoreland Conglomerate.|Immature ferruginous meta-greywacke (lower greenschist facies) sampled.|
13528|Murphy Metamorphics|69417|5|Briefly described|p2:4-5, 9|Orosirian|Orosirian|Murphy Province. Maximum depositional age.|1853 Ma (Hollis et al., 2009).|||Is intruded by Nicholson Granite Complex. Is overlain unconformably by Cliffdale Volcanics.||12-JUL-16
13528|Murphy Metamorphics|69423|4|Described|p8:1-5, 7|Orosirian|Orosirian|Murphy Inlier, Murphy Province. Possible stratigraphic equivalent of Finniss River Group (Pine Creek Orogen) and Warramunga Formation (Warramunga Province). Isoclinally folded; dips vertically or steeply to N. LA-ICPMS detrital zircon maximum deposition age; Hollis et al. (2010). Minimum depositional age of c.1850 Ma from stratigraphic relationships. Hosts the Coanjula microdiamond occurrence; also minor uranium occurrences in the W of the Inlier near the contact with the Nicholson Granite Complex.|<1853 +/- 4 Ma to c.1850 Ma.|||Is overlain unconformably by Cliffdale Volcanics. Is intruded by Nicholson Granite Complex.|A succession of greenschist-facies metamorphosed shale and greywacke: phyllite, schist and quartzite. A 5m-thick banded ironstone is present locally. Numerous quartz veins. Banded chert and hematitic ironstone, pyritic and graphitic at depth.|12-JUL-16
13528|Murphy Metamorphics|69430|5|Briefly described|p15:11, 51|||Hosts minor U mineralisation associated with faults and fractures.||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).||12-JUL-16
13528|Murphy Metamorphics|69433|5|Briefly described|p18:2, 4-5|||Murphy Province. Basement to the Lawn Hill Platform succession.||||Is overlain unconformably by Carrara Range and Benmara Groups (Lawn Hill Platform).||12-JUL-16
13528|Murphy Metamorphics|69434|5|Briefly described|p19:1, 4-5|Paleoproterozoic|Paleoproterozoic|Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||Is overlain unconformably by Crow Formation (South Nicholson Group).||12-JUL-16
13528|Murphy Metamorphics|69510|5|Briefly described|piii, p17-19, 21|||SHRIMP U-Pb zircon maximum depositional age. The intrusion at 1846 +/- 6 Ma provides a minimum depositional age for the sedimentary protolith. Previous age determinations (c.1870 Ma and c.1853 Ma) are mentioned.|1864.3 +/- 5.0 Ma (Kositcin et al., 2014).|||Is intruded by the Nicholson Granite.|Includes lithic greywacke interlayered with minor banded shale and quartzwacke.|
13528|Murphy Metamorphics|69591|5|Briefly described|p30-31, p58|||Camooweal-Murphy Domain. Does not crop out in Qld, but is inferred in the subsurface of the Murphy Tectonic Ridge. Considered part of the same depositional package as the Murphy and Yaringa Metamorphics. Minimum age (Page et al., 2000) from intrusion.|>1856 Ma.|||Is intruded by Nicholson Granite.|Quartz-albite-muscovite-biotite schist; gneiss, phyllite and migmatite.|
13528|Murphy Metamorphics|69673|6|Mentioned|p3 fig 2, p51|Orosirian|Orosirian|||||||
13528|Murphy Metamorphics|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||||Is overlain unconformably by Wire Creek Sandstone (Tawallah Group equivalent). Is intruded by Nicholson Granite Complex.|Undivided: metasedimentary rocks, commonly sheared and brecciated; quartz-albite-mica schist. Separately mapped: metasiltstone and metashale; immature metasandstone, poorly sorted, fine- to coarse-grained, micaceous.|
13528|Murphy Metamorphics|71592|5|Briefly described|Appendix A.|||Murphy Region.|1853+/-4 Ma (MDA: U-Pb zircon LA-ICPMS).||||Greywacke.|
13528|Murphy Metamorphics|71606|5|Briefly described|p137|Orosirian|Orosirian|Murphy Tectonic Ridge and South Nicholson Basin.||||Overlain unconformably by Cliffdale Volcanics and Wire Creek Sandstone, and Nicholson Granite. Equivalent to Yaringa Metamorphics.||
13528|Murphy Metamorphics|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
13528|Murphy Metamorphics|72526|5|Briefly described|p8 Fig.1.3, p6 Fig.1.2.|Orosirian|Orosirian|Shown as being located in the west and central part of the South Nicholson Basin and the Southeastern McArthur Basin.||||Shown as underlying Cliffdale Volcanics.||
13528|Murphy Metamorphics|72527|4|Described|p3, p5, p7, 9, 161, 181, p184-191, p192|Paleoproterozoic|Paleoproterozoic|Murphy Province. Sample gives 1874+/-7 Ma max.dep.age. Previous detrital zircon geochronology results: 1867+/-7 Ma, 1864+/-5 Ma, 1852+/-4 Ma. Minimum age constrained by overlying and intruding units. Considered to represent a succession of turbidites prior to metamorphism. The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds. Correlated with Burrell Creek Formation, Yaringa Metamorphics, Inverway Metamorphics, Lander Rock Formation. See also p193 Fig.9.1, p194.|Depositional age 1867-1845 Ma.|||Unconformably underlies Wire Creek Sandstone, Cliffdale Volcanics. Extensively intruded by Nicholson Granite complex.|Greenschist-facies shales, schists, meta-siltstones, meta-arenites, meta-greywackes, meta-volcanics and rare banded ironstone.|
13528|Murphy Metamorphics|72912|5|Briefly described|p5 Fig.3, p20.|Orosirian|Orosirian|Basement rocks located in the west part of the South Nicholson Basin and the Southeastern McArthur Basin.|c. 1850 Ma|||Shown as underlying Cliffdale Volcanics. Faulted against South Nicholson Group at Benmara Fault.||15-MAR-21
13528|Murphy Metamorphics|72919|6|Mentioned|p5-7, p11, p16|Paleoproterozoic|Paleoproterozoic|Murphy Province, North Australian Craton.||||Intruded by Nicholson Granite Complex. Unconformably overlain by Cliffdale Volcanics.||
13528|Murphy Metamorphics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin and South Nicholson Basin region.||||||
13528|Murphy Metamorphics|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: Murphy Province.||||||
13528|Murphy Metamorphics|73089|5|Briefly described|p32, p34|||Murphy Province. Contains dominant detrital zircon age components of 1867 +/- 7 and 1853 +/- 4 Ma, with a smaller proportion of early Paleoproterozoic to Neoarchean grains. Unconformably overlain by 1851 +/- 3 Ma felsic volcanic rocks.|||||Turbiditic shale and greywacke with lesser ironstone, quartzite and chert.|
13528|Murphy Metamorphics|73427|4|Described|p3, p5-6, p12-14, App.A|Orosirian|Orosirian|North Australian Craton, Murphy Inlier/Murphy Province. Also exposed in the Carrara Range Inlier. Represents turbidity flows and chemical sediments deposited in a deep marine or shelf setting. Previous maximum depositional ages include 1874 +/- 7 Ma (Kositcin and Carson, 2019) and 1867 +/- 7 Ma (Hanley, 1996). Sampled for monazite U-Pb dating to constrain deformation and metamorphism. Deformed and metamorphosed during the Murphy Event (D1/M1: 1860-1855 Ma); isoclinally folded about east-trending axes and dip steeply to the north; greenschist-facies metamorphism. A second episode of ductile deformation and metamorphism (D2/M2) occurred during the waning stage of, or after, 1855-1845 Ma igneous activity.|ca 1860 Ma|||Crosscut by Nicholson Granite.|Shale, siltstone, greywacke, schist and felsic volcanic rocks, with rare banded ironstone and calc-silicate rock.|
13528|Murphy Metamorphics|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|||||Metamorphics.|
13577|Murta Formation|13497|5|Briefly described|p115, p115 fig 6.33, p130, p138|Early Cretaceous|Early Cretaceous|Eromanga Basin, Dullingari Field. Deposited in a high-sinuosity fluvial, overbank, lacustrine or proximal deltal environment. This formation is an oil source rock. Oil and gas reservoir. See also p138 fig 8.17, p141, p142, p146, p151 fig 9.23, p152 fig 9.26, p170, p171, p183, p188, p216.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstones, siltstone, shale and minor coal.|
13577|Murta Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||||||
13577|Murta Formation|22839|6|Mentioned|P33|||||||||
13577|Murta Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlain by Cadna-owie Formation, underlain by Namur Sandstone.||||||17-JAN-08
13577|Murta Formation|22912|5|Briefly described|33|||Geological Province: Eromagna Basin.||||||17-JAN-08
13577|Murta Formation|23054|6|Mentioned|Fig5p22|Valanginian|Berriasian|||||||
13577|Murta Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Includes McKinlay Member.||||||
13577|Murta Formation|23155|3|Fully described|p28 & Fig 15 on p28|Early Cretaceous|Early Cretaceous|The Murta Formation is Early Cretaceous (Neocomian) in age, from spore pollen determination.  See p28 for details of type section etc.||||||
13577|Murta Formation|23356|5|Briefly described|26 Tab.2|Neocomian|Neocomian|||||||
13577|Murta Formation|23375|4|Described|Fig2 p265|Valanginian|Berriasian|Laterally equivalent to upper Hooray Sandstone. In the Eromanga Basin.||||||17-JAN-08
13577|Murta Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the McKinlay Member.  Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13577|Murta Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Contains the McKinlay Member. Geological Province: Eromanga Basin.||||||
13577|Murta Formation|37287|6|Mentioned|p36|||||||||
13577|Murta Formation|41705|6|Mentioned|p128|||||||||
13577|Murta Formation|42071|6|Mentioned|p117|||||||||
13577|Murta Formation|44133|4|Described|p111, 104 Fig. 9.11|Neocomian|Neocomian|Geological Province: Eromanga Basin. Formerly upper part of the Mooga Formation known as the Murta Member. Overlies and intertongues with McKinlay Member and Namur Sandstone. Overlain transitionally by Cadna-owie Formation.||||||08-MAY-13
13577|Murta Formation|60717|5|Briefly described|p40 Fig. 2, p42|Early Cretaceous|Late Jurassic|Contains the McKinlay member. Overlies Westbourne Formation; overlain by Cadna-owie Formation; interfingers partially with Algebuckina Sandstone. Geological Province: Eromanga  Basin.||||||31-JAN-08
13577|Murta Formation|61614|5|Briefly described|p289, p294, p295, p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Largely carbonaceous siltstones deposited in lacustrine and paralic environments.||||||17-MAR-09
13577|Murta Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13577|Murta Formation|62028|6|Mentioned|p11|||May provide a regional seal.||||||26-FEB-08
13577|Murta Formation|62029|5|Briefly described|p15 Fig. 4|||See also Murta Member.||||||08-APR-08
13577|Murta Formation|62537|6|Mentioned|p191 Fig.2, p192.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Significant hydrocarbon source potential.||||Overlies Birkhead Formation. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|63979|2|Defined|p44, Fig. 44|Valanginian|Berriasian|Supersedes "Murta Member" in SA; also now extended to Qld. Passes laterally into upper part of Hooray Sst. Prev. referred to as Murta Member of Mooga Formation by petroleum companies.Detailed desc./explans. lithology/nomenclature included||||Laterally equivalent to upper part of Hooray Sandstone.||09-APR-13
13577|Murta Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses relatively low hydrocarbon source potential.||||||07-FEB-11
13577|Murta Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Namur Sandstone. Overlain by Cadna-owie Formation.||||||08-MAR-12
13577|Murta Formation|65489|5|Briefly described|p15, p47, p49, p55, p73, p96, p132, p152|Early Cretaceous|Early Cretaceous|See also p154-158, p160. Eromanga Basin. 60m thick. Hydrocarbon source rock. Oil reservoir accounting for 10% of the Basin's production. Intraformational shale regional seal.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.|Lacustrine turbidite sandstones.|
13577|Murta Formation|65925|5|Briefly described|Appendix 2.||||||||Dark grey, argillaceous and carbonaceous siltstone with interbedded fine- to very fine-grained sandstone.|
13577|Murta Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|66623|5|Briefly described|pp240-242.|||Not identified in outcrop for this study, although recognised in borehole sections. Largely non-marine.|||||Interbedded siltstone, shale, very fine-grained sandstone and minor medium- to coarse-grained sandstone.|
13577|Murta Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|67561|5|Briefly described|p52 Fig.2|Valanginian|Berriasian|Australian Spore-Pollen zonation: australiensis.||||||
13577|Murta Formation|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Subsurface only.|||Includes McKinlay Member at base.|Overlies Namur Sandstone. Is overlain conformably by Parabarana Sandstone and Cadna-owie Formation.|Dark grey laminated carbonaceous siltstone, graded beds, ripple marks with interbeds of fine-grained to locally coarse-grained sandstone, ripple laminated, bioturbated; carbonate cemented layers near top; diagenetic siderite common.|
13577|Murta Formation|68731|6|Mentioned|pp209-211|||||||||
13577|Murta Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
13577|Murta Formation|69019|5|Briefly described|p85 Fig.21.|Valanginian|Berriasian|Southern Eromanga Basin.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|69023|4|Described|p79, p86, p89 Fig.20, p92, p191-192|Valanginian|Berriasian|Defined by Nugent (1969) as Murta Member, part of the Mooga Formation; later elevated to Formation status (Callen et al.,1994; Gravestock et al., 1995) and the Mooga Formation was discarded. The McKinlay Member (Mount, 1982) became a Member of the Murta Formation. Eromanga Basin. Thickness from ~33 to >53m. Stratigraphic wells intersection data.|||Includes McKinlay Member.|Overlies Namur and Algebuckina Sandstones. Passes laterally into Algebuckina Sandstone. Is overlain gradationally by Cadna-owie Formation.|Dark grey argillaceous and carbonaceous siltstone interbedded with fine- to very fine-grained sandstone, diagenetic siderite and calcite nodules and layers; overlain by thinly interbedded siltstone and sandstone; passing up into dark grey siltstone.|
13577|Murta Formation|69454|6|Mentioned|p38:13|||The uppermost shale of previous usage (eg Ambrose and Heugh, 2010) was referred to basal Cadna-owie Formation by Gray et al. (2002). This Formation, with the underlying Namur Sandstone (in the Cooper Basin), are equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13577|Murta Formation|69457|5|Briefly described|p41:3-5, 7|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain conformably by Cadna-owie Formation.||12-JUL-16
13577|Murta Formation|69594|5|Briefly described|p519, p526-528, p531-532, p573|Hauterivian|Berriasian|Eromanga Basin; mostly in SA. Generally 50-60m thick; possibly >100m locally. Brackish environment. A significant hydrocarbon reservoir; has hydrocarbon source potential.||||Overlies Namur Sandstone; conformably overlies upper Namur Sandstone. Is overlain conformably/transitionally by Cadna-owie Formation. Lateral equivalent of (upper) Hooray Sandstone.|Interbedded and interlaminated sublabile to quartzose sandstone, silty sandstone, siltstone and lesser mudstone, intraformational conglomerate and coal.|
13577|Murta Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Namur Sandstone, overlain by Cadna-owie Formation||
13577|Murta Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|69797|5|Briefly described|p17 incl Fig.2|Early Cretaceous|Early Cretaceous|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are organic-rich shales and siltstones of the Murta Formation, the coals and carbonaceous shales of Birkhead Formation, and highly carbonaceous shales of Poolowanna Formation. Geol. Prov: Eromanga Basin.||||||17-JAN-17
13577|Murta Formation|69946|2|Defined|p11, p17-19, p56-58, p86-92|Early Cretaceous|Early Cretaceous|Siltstone and shale in the upper part of the Mooga Formation were defined as Murta Member by Nugent (1969); raised to Formation status by Gravestock et al. (1995). Equivalent to the upper Hooray Sandstone in Qld. Type section is the interval 1469.14 - 1526.13m in Dullingari North 1. Up to >90m thick. Wireline log correlations. Sedimentary facies log.|||Includes McKinlay Member.|Overlies and intertongues with Namur Sandstone. Is overlain gradationally by Cadna-owie Formation. Intertongues with Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey very fine- to fine-grained sandstone; minor medium- and coarse-grained sandstone. Diagenetic siderite nodules and layers.|
13577|Murta Formation|69947|5|Briefly described|p3, p8, p13 Fig.7.2, p29-31 Figs.7.18-20|Early Cretaceous|Early Cretaceous|Eromanga Basin. Widespread meandering fluvial, floodplain and lacustrine facies. Represents two major transgressive-regressive cycles; illustrated by a well log from the Maxwell Field.|||McKinlay Member.|Conformably overlies Namur, Hooray Sandstones. Is overlain conformably by Cadna-owie Formation.|Sandstone, siltstone.|
13577|Murta Formation|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|70821|5|Briefly described|p31|||Previously part of the [obsolete] "Lower Hooray Sandstone". 44 m thick interval, between 395 and 439 m in Weilmoringle 1 well. See also Murta Member p21||||Overlies Namur Sandstone.||02-DEC-16
13577|Murta Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstone, siltstone, shale and coal.|
13577|Murta Formation|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13577|Murta Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Algebuckina Sandstone, Namur Sandstone and the McKinlay Member.||24-OCT-19
13577|Murta Formation|71342|6|Mentioned|Ch 1 p6, Ch 1 p19, Ch4 p9, Ch5 p12|Cenomanian|Berriasian|Originally defined by Nugent (1969) as siltstone and shale in the upper part of the Mooga Formation. Gravestock et al, (1995) elevated the name to Murta Formation. This unit is equivalent to the upper Hooray Sandstone in Queensland. The type section is in Dullingari North 1 (Mount, 1981). Diagenetic siderite nodules and layers produce distinctive spikes on sonic and density logs. This unit has a maximum thickness >90m in the Nappamerri Trough. Age based partly on palynology. Interpreted to have been deposited in open lacustrine, lacustrine fan delta, distributary channel and lacustrine shoreline environments. A brackish to marine environment is suggested for the upper parts of this formation. Spore-pollen zone is given in Ch5 p57. A complete sedimentary facies log is given in Ch5 p88. Source rock characteristics are described in detail in Ch8 (p6). Forms a seal over the Namur Sandstone. Oil is produced from a very thin by extensive, high-permeability shoreface sand. See also  Ch5 p17-p18, Ch5 p30, Ch5 p32, Ch5 p57-p58, Ch5 p85-p92, Ch6 p5, Ch6 p7, Ch7 p3, Ch7 p8, Ch7 p11, Ch7 p13, Ch7 p29-p31, Ch8 p2, Ch8 p5-p6, Ch8 p8, Ch8 p10, Ch8 p17, Ch8 p22, Ch10 p3, Ch10 tbl 10.1, Ch10 p8, Ch10 p14, Ch10 p17-p20, Ch11 p2-p5, Ch11 p7-p8, Ch11 p17, Ch12 p5, Ch13 p2-p3, Ch13 p7, Ch13 p9-p10, Ch13 p25-p28, Ch13 p31, Ch13 p33, Ch14 p5.|||Includes the McKinlay Member.|Intertongues with and overlies the McKinlay Member and the Namur Sandstone. Conformably overlain by the Cadna-owie Formation. Intertongues with and is equivalent to the Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey, very fine to fine-grained sandstone and minor medium and coarse-grained sandstone.|
13577|Murta Formation|71863|6|Mentioned|p5|Hauterivian|Berriasian|Eromanga Basin.||||Overlies Namur Sandstone, overlain by Cadna-owie Formation.||
13577|Murta Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential. Oil flows >2000 bpd in Dullingari North 1 (in SA).||||||
13577|Murta Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.|||McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie FZ.||
13577|Murta Formation|73251|6|Mentioned|p55-56, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in freshwater lacustrine conditions. Capable of generating hydrocarbons (marginally mature for liquid hydrocarbon generation); constitutes the most shallow-lying and demonstrably effective petroleum source within the stacked Warburton, Cooper, and Eromanga Basins. Partly self-sourcing and likely to have contributed to hydrocarbon accumulations within the overlying Namur Sandstone and Cadnaowie Formation. Depositional environments included lacustrine turbidites, deltas, and shoreface.||||Underlain by and equivalent to Namur Sandstone. Overlain by [and equivalent to?] Cadna-owie Formation.||
13577|Murta Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
13586|Murteree Shale|13497|3|Fully described|iv, v, xi, p58, p69 fig 6.1|Kungurian|Artinskian|Cooper Basin. Defined by Gatehouse (1972), name is derived from Lake Murteree. Originally included in the Moomba Formation before Gatehouse raised it to formation status. A type section from core is mentioned. Is relatively uniform in thickness with a maximum thickness of 80m in the Nappamerri Trough. Interpreted to have been deposited in a broad, fresh-water lake. This unit forms an important regional seal over the Patchawarra Formation. Wireline log results are discussed. See also p70, p89, p93-p97, p101-p102, p117, p129, p131, p132, p150-p151, p160, p163, p170-p175.||Gidgealpa Group||Conformably overlies and intertongues with the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Black to dark grey-brown argillaceous siltstone and fine-grained sandstone. Fine-grained pyrite and muscovite are charateristic and carbonaceous siltstone also occurs.|
13586|Murteree Shale|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
13586|Murteree Shale|22839|6|Mentioned|P33|||||||||
13586|Murteree Shale|22883|6|Mentioned|P29|||||||||
13586|Murteree Shale|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Parent - Gidgealpa Group.||||||
13586|Murteree Shale|23155|4|Described|p19|Early Permian|Early Permian|Spore and pollen indicate an Early Permian age. The unit is wide spread on STRZELECKI and relatively uniform in thickness (50+/- 25m).||||||
13586|Murteree Shale|23340|6|Mentioned|12|||||||||
13586|Murteree Shale|23375|4|Described|Fig2 p265,285||Artinskian|In the Cooper Basin.||||||17-JAN-08
13586|Murteree Shale|23832|4|Described|p329|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
13586|Murteree Shale|24199|5|Briefly described|p512 Fig.2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
13586|Murteree Shale|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Patchawarra Formations; underlies the Epsilon Formation.  Geological Province: Cooper Basin.  See also p132.||||||
13586|Murteree Shale|29387|6|Mentioned|Table 2|||Refers to Gatehouse 1972.||||||
13586|Murteree Shale|29391|6|Mentioned|Table 5|||See p23.||||||
13586|Murteree Shale|29721|6|Mentioned|p137|||||||||
13586|Murteree Shale|30540|6|Mentioned|Fig.6|||||||||
13586|Murteree Shale|30544|6|Mentioned|p53|||Map legend||||||
13586|Murteree Shale|30825|6|Mentioned|p37|||||||||
13586|Murteree Shale|30873|2|Defined|p14|Permian|Permian|Part of Gidgealpa Group.||||||17-JAN-08
13586|Murteree Shale|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
13586|Murteree Shale|32696|6|Mentioned|Fig.4|||See also Figs 6 & 7||||||
13586|Murteree Shale|33074|6|Mentioned|p260|||||||||
13586|Murteree Shale|33331|6|Mentioned|p42|||||||||
13586|Murteree Shale|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
13586|Murteree Shale|33976|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|34839|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|35067|6|Mentioned|Fig.4|||||||||
13586|Murteree Shale|35068|6|Mentioned|Fig.3|||Discussed P58.||||||
13586|Murteree Shale|35279|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
13586|Murteree Shale|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
13586|Murteree Shale|35845|4|Described|p23|||Lithology and depositional environments. See also p62.||||||17-JAN-08
13586|Murteree Shale|36099|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|36910|6|Mentioned|p62|||||||||
13586|Murteree Shale|36917|6|Mentioned|Fig.1|||||||||
13586|Murteree Shale|37855|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|37917|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|38977|6|Mentioned|p1423|||||||||
13586|Murteree Shale|39252|5|Briefly described|p20|||||||||
13586|Murteree Shale|39254|5|Briefly described|p46|||||||||
13586|Murteree Shale|39261|6|Mentioned|Fig. 9|||||||||
13586|Murteree Shale|39264|6|Mentioned|Fig. 13|||||||||
13586|Murteree Shale|39276|6|Mentioned|Fig. 2|||||||||
13586|Murteree Shale|39445|5|Briefly described|Table 8|||||||||
13586|Murteree Shale|39478|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|39494|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|40030|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|40249|6|Mentioned|p45|||||||||
13586|Murteree Shale|40544|6|Mentioned|Fig.4|||||||||
13586|Murteree Shale|41060|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|41099|6|Mentioned|p190|||||||||
13586|Murteree Shale|41131|5|Briefly described|Table 1|||||||||
13586|Murteree Shale|41164|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|41183|6|Mentioned|Fig.3 p308|||||||||
13586|Murteree Shale|41189|6|Mentioned|p260|||||||||
13586|Murteree Shale|41198|6|Mentioned|Table 1|||||||||
13586|Murteree Shale|41214|6|Mentioned|Fig.3|||||||||
13586|Murteree Shale|41247|6|Mentioned|Fig.5|||||||||
13586|Murteree Shale|41267|6|Mentioned|Fig.2|||||||||
13586|Murteree Shale|41288|6|Mentioned|p158|||||||||
13586|Murteree Shale|41290|6|Mentioned|Fig.8|||||||||
13586|Murteree Shale|41595|6|Mentioned|p31|||||||||
13586|Murteree Shale|41720|6|Mentioned|p373|||||||||
13586|Murteree Shale|42085|6|Mentioned|Fig.2 P374|||||||||
13586|Murteree Shale|42395|5|Briefly described|Fig.13 P83|||||||||
13586|Murteree Shale|42746|5|Briefly described|p6|||||||||
13586|Murteree Shale|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
13586|Murteree Shale|43002|5|Briefly described|Fig.2,p135|||||||||
13586|Murteree Shale|43018|5|Briefly described|Table 1,p386|||||||||
13586|Murteree Shale|43105|5|Briefly described|p14|||||||||
13586|Murteree Shale|43570|5|Briefly described|Fig.2,p535,544|Kungurian|Artinskian|||||||
13586|Murteree Shale|43628|6|Mentioned|Fig.3||Early Permian|||||||
13586|Murteree Shale|44133|4|Described|p65 Fig. 8.3, 84|Kungurian|Artinskian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlies: Patchawarra Formation. Up to 80m thick. Conformably underlies: Epsilon Formation.||||||
13586|Murteree Shale|46849|6|Mentioned|Fig. 7|||||||||
13586|Murteree Shale|60386|6|Mentioned|p296|Artinskian|Artinskian|Cooper Basin. Non-marine.||||||
13586|Murteree Shale|60717|5|Briefly described|p40 Fig. 2|Kungurian|Artinskian|Of Gidgealpa Group. Overlies Patchawarra Formation; underlies Epsilon Formation. Thickness: 80m. Geological Province: Cooper Basin.||||||31-JAN-08
13586|Murteree Shale|61614|6|Mentioned|p290 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
13586|Murteree Shale|61615|5|Briefly described|p302, p302 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Conformbaly underlain by Parchawarra Formation. Geological Province: Cooper Basin.||||||07-FEB-11
13586|Murteree Shale|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
13586|Murteree Shale|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
13586|Murteree Shale|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|63832|6|Mentioned|p131 fig 2|Cisuralian|Cisuralian|Of Cooper Basin.||||||14-MAR-14
13586|Murteree Shale|63978|2|Defined|p13, Fig. 3|Early Permian|Early Permian|Originally interp. by Kapel (1972) as lower third of Moonbi Fm. Conformably overlies Patchawarra Fm; conformably underlies Epsilon Fm. Dark grey-brown to black, laminated, argillaceous siltstone + lesser fine-gr.sandstone (more lith. incl.). Thick: 80m.||||||07-FEB-11
13586|Murteree Shale|64048|5|Briefly described|p63, p64 Tb. 2|||Geological Province: Cooper Basin. Acts as the seal for Patchawarra Formation reservoirs.||||||07-FEB-11
13586|Murteree Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Permian|Middle Permian|Cooper Basin.||||Overlies the Patchawarra Formation; underlies the Epsilon Formation.||11-DEC-15
13586|Murteree Shale|64631|5|Briefly described|p44 Fig.2.|Kungurian|Artinskian|Cooper Basin. Biostratigraphic age control for base and top.||||Overlies Patchawarra Sandstone. Showns as overlain by Roseneath/Epsilon.||
13586|Murteree Shale|64665|5|Briefly described|p53 Fig.2.|Early Permian|Early Permian|Cooper Basin.||||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|65489|5|Briefly described|p45-46, p48-49, p96, p131-132, p143|Kungurian|Artinskian|Cooper Basin. 80m thick. Relatively little hydrocarbon source potential. Seal for Patchawarra Formation.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation and Roseneath Shale.|Lacustrine shale unit.|
13586|Murteree Shale|65925|5|Briefly described|Appendix 2.||||||||Siltstone, grey-green, shaly, with thin lenses of fine-grained sandstone. Lacustrine.|
13586|Murteree Shale|67402|5|Briefly described|p90, p90 fig CPR4||BD|Cooper Basin. 50-100m thick. Distal lacustrine deposits. Forms regionally extensive seal to the Patchawarra Formation. See also p91 tbl CPR1, p92, p93, p96, p98, p101 tbl CPR2.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.|Predominantly laminated, argillaceous siltstone and minor thinly bedded, fine-grained sandstones.|
13586|Murteree Shale|68068|5|Briefly described|Map legend|Early Permian|Early Permian|Cooper Basin (subsurface only). Lacustrine, cyclic oxic to anoxic conditions.||Unit in Gidgealpa Group.||Conformably overlies Patchawarra Formation. Is overlain conformably by Epsilon Formation.|Dark grey, interbedded, carbonaceous mudstone and siltstone with minor sandstone, characteristically fine-grained variably pyritic and muscovite; laminated and calcareous.|
13586|Murteree Shale|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian|Cisuralian|Gatehouse (1972). Along with the Epsilon Formation and Roseneath Shale, the Murteree Shale replaces the Moomba Formation. < 80 m thick. Deposited in a large freshwater lake, with restricted circulation. Contains Kungurian palynofloras (Price 1997).||Of the Gidgealpa Group.||Conformably underlain by the Patchawarra Formation. Interdigitates with the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Comprises dark, laminated, argillaceous siltstone and lesser fine sandstone with carbonaceous material, muscovite and fine pyrite.|
13586|Murteree Shale|69023|4|Described|p79, p81, p82 Fig.18, p84-85, p191-192|Permian|Permian|Defined by Gatehouse (1972). Widespread in Cooper Basin. 50 +/- 25m thick. Hydrocarbon source rocks. Lacustrine. Has high gamma ray and density values on wireline logs. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Conformably overlies Patchawarra Formation. Is overlain by Epsilon Formation.|Black to dark grey-brown, laminated, argillaceous siltstone and fine-grained sandstone; disseminated carbonaceous matter, fine-grained pyrite and muscovite are characteristic.|
13586|Murteree Shale|69454|5|Briefly described|p38:4|Kungurian|Artinskian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
13586|Murteree Shale|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Epsilon Formation, overlies Patchawarra Formation||
13586|Murteree Shale|69797|5|Briefly described|p17 Fig.2|Early Permian|Early Permian|Age: Artinskian - Kungurian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
13586|Murteree Shale|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Artinskian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
13586|Murteree Shale|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|70823|4|Described|iv, p1, p3, p6|Kungurian|Kungurian|Cooper Basin. Hosts shale gas plays. Seismic reflection characteristics briefly discussed. Up to 90m thick. Deposited in a deep lacustrine environment. This unit contains potential source rock facies. See also p14-p15, p25-p27, p38, p40-p41, p53, p58-p59, p64, p78, p82-p83.||Gidgealpa Group||Conformably overlies and intertongues the Patchawarra Formation. Conformably overlain by the Epsilon Formation. Unconformably overlain by the Toolachee Formation.|Black to dark grey-brown argillaceous siltstone with minor fine-grained sandstone.|
13586|Murteree Shale|70824|4|Described|p1, p3, p7-p9, p28|Kungurian|Kungurian|Cooper Basin. Hosts shale gas plays. Deposited in a lacustrine environment. This unit has an average thickness of 50m but in the Nappamerri trough reaches a maximum thickness up to 90m. Forms a seal over the Patchawarra Formation. Outcrop characteristics and areal extent discussed briefly in addition to source rock geochemistry. See also p30-p32, p59-p65, p108-p109, p113, p122.||||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.|Black to dark grey-brown argillaceous siltstone with minor fine-grained sandstone.|
13586|Murteree Shale|70946|5|Briefly described|p1087, p1089-1091, p1096|Permian|Early Permian|Cooper Basin. Hosts shale gas plays. Widespread unit. Up to 92m thick, thinning northwards. HyLogging was combined with XRD and core petrology to target fracture stimulation. Deposited in lacustrine with interbedded fluvio-deltaic transgressive/regressive shoreface environments.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.|Siltstones, siliceous (and sideritic in part) mudstones.|08-OCT-18
13586|Murteree Shale|71265|5|Briefly described|p589|Kungurian|Kungurian|Cooper Basin.||Gidgealpa Group.||Overlies Patchawarra Formation. Is overlain by Epsilon Formation.||
13586|Murteree Shale|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36|Artinskian|Artinskian|Cooper Basin. Deposited in a lacustrine environment.  Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p45, Ch5 p54, Ch7 p13, Ch10 p15, Ch10 p18-p19.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.||
13586|Murteree Shale|71701|5|Briefly described|p155|Kungurian|Kungurian|Cooper Basin.||Gidgealpa Group||Overlies the Patchawarra Formation. Overlain by the Epsilon Formation.||
13586|Murteree Shale|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Cooper Basin.||||||
13586|Murteree Shale|72297|6|Mentioned|p742|||Cooper Basin. Acts as a regional seal.||||||
13586|Murteree Shale|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments.||||||
13586|Murteree Shale|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface environment.||||||
13586|Murteree Shale|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Fluviodeltaic with local transgressive/regressive shoreface depositional environments. Hydrocarbon source rock.||Gidgealpa Group||Underlain by Patchawarra Formation. Overlain by and equivalent to Epsilon Formation.||
13586|Murteree Shale|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin.||||Underlain by Patchawarra Formation. Overlain by Roseneath Shale. Equivalent to Epsilon Formation.||
13586|Murteree Shale|73479|5|Briefly described|p156 Fig.2, p159, p163, p166|Permian|Permian|Cooper Basin. Fluvio-deltaic/shoreface depositional environment. Highly efficient regional seal, eroded along western margin of the basin.|ca 264 Ma|||Overlies Patchawarra Formation||
13586|Murteree Shale|73495|6|Mentioned|p497, p499|Guadalupian|Guadalupian|Cooper Basin. Part of the REM succession.||||Underlain by Patchawarra Formation. Overlain by Epsilon Formation.||
13609|Musket Flat Granodiorite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
13609|Musket Flat Granodiorite|30654|6|Mentioned|p56|||||||||
13609|Musket Flat Granodiorite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
13609|Musket Flat Granodiorite|35161|6|Mentioned|p592|||||||||
13609|Musket Flat Granodiorite|36954|6|Mentioned|p114|||||||||
13609|Musket Flat Granodiorite|37118|6|Mentioned|p317|||||||||
13609|Musket Flat Granodiorite|39445|5|Briefly described|Table 12|||||||||
13609|Musket Flat Granodiorite|39505|6|Mentioned|p180|||||||||
13609|Musket Flat Granodiorite|41738|6|Mentioned|p173|||||||||
13609|Musket Flat Granodiorite|41778|6|Mentioned|Fig.2|||||||||
13609|Musket Flat Granodiorite|42894|6|Mentioned|p23|||||||||
13609|Musket Flat Granodiorite|45440|2|Defined|p.21,28,31,57,58-88||Triassic|Tb.1. Of many pages.||||||
13609|Musket Flat Granodiorite|63821|4|Described|p32|Late Triassic|Late Triassic|Age: 221Ma (K-Ar biotite). Intrudes Brooweena Formation. Comprises hornblende-biotite granodiorite, granite and diorite.||||||07-FEB-11
13609|Musket Flat Granodiorite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
13609|Musket Flat Granodiorite|68679|5|Briefly described|p428, p430|Late Triassic|Late Triassic|NE of Mungore Cauldron, northern New England Orogen. May be continuous at depth with Broomfield Granite.|221 Ma (K-Ar biotite: Webb and McDougall, 1967).|||Intrudes Gympie Group and Brooweena Formation. Is overlain unconformably by Myrtle Creek Sandstone.|Medium-grained hornblende-biotite granodiorite and marginal phases of granite and diorite.|
13635|Myally Subgroup|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546||||||
13635|Myally Subgroup|22585|5|Briefly described|P739, Fig1|||||||||
13635|Myally Subgroup|22644|5|Briefly described|5|||Geological province: Mount Isa Basin. Overlain by Quilalar Formation||||||18-JAN-07
13635|Myally Subgroup|23031|5|Briefly described|24|||Geological province: Mount Isa Fold Belt. Underlain by Leander Quartzite, Eastern Creek Volcanics.||||||13-NOV-06
13635|Myally Subgroup|23073|5|Briefly described|p744 (fig 2), p748|||||||||
13635|Myally Subgroup|23393|5|Briefly described|p18, p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group.  Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
13635|Myally Subgroup|23395|4|Described|p384 Fig.2|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|23396|5|Briefly described|p407 Fig.2|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|23397|6|Mentioned|p467|||||||||
13635|Myally Subgroup|23399|5|Briefly described|p500|||||||||
13635|Myally Subgroup|23408|6|Mentioned|p511, p515|||Underlies Torpedo Creek Quartzite.||||||15-JUN-09
13635|Myally Subgroup|23466|5|Briefly described|p265|||||||||
13635|Myally Subgroup|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt. Of the Haslingden Group.||||||
13635|Myally Subgroup|23767|5|Briefly described|p1954 Fig. 1a|||Maximum thickness: ~2500m.   Geological Province: Leichhardt Superbasin. See also p1955.||||||
13635|Myally Subgroup|23965|4|Described|p1296|Paleoproterozoic|Paleoproterozoic|Of Haslingden Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier. Of the Haslingden Group.||||||
13635|Myally Subgroup|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
13635|Myally Subgroup|24419|5|Briefly described|p16, p13 Fig. 5, p12 Fig. 4|Proterozoic|Proterozoic|Formerly the Judenan beds. Of the Haslingden Group.  Conformably overlies Mount Guide Quartzite and Eastern Creek Volcanics. Geological Province: Leichardt River Subprovince and Lawn Hill Subprovince. See also p15 Fig. 6.||||||18-JAN-07
13635|Myally Subgroup|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Eastern Creek Volcanics. Overlain by Quilalar Formation.||||||
13635|Myally Subgroup|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.||||||25-AUG-04
13635|Myally Subgroup|30534|6|Mentioned|p303|||Revision of name||||||
13635|Myally Subgroup|30535|6|Mentioned|p403|||||||||
13635|Myally Subgroup|33900|4|Described|p12|||Mention p10.||||||13-NOV-06
13635|Myally Subgroup|35074|6|Mentioned|Fig.2|||||||||
13635|Myally Subgroup|35286|6|Mentioned|Fig.17|||||||||
13635|Myally Subgroup|35295|6|Mentioned|Fig.2|||||||||
13635|Myally Subgroup|35369|6|Mentioned|Table 1|||Stratigraphy||||||
13635|Myally Subgroup|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|36548|6|Mentioned|p513|||||||||
13635|Myally Subgroup|37459|6|Mentioned|p423|||||||||
13635|Myally Subgroup|37462|6|Mentioned|p266|||||||||
13635|Myally Subgroup|37568|5|Briefly described|p81|||See also p85.||||||13-NOV-06
13635|Myally Subgroup|37569|6|Mentioned|p91|||||||||
13635|Myally Subgroup|38232|6|Mentioned|p84|||||||||
13635|Myally Subgroup|38233|5|Briefly described|Table 1|||||||||
13635|Myally Subgroup|38235|6|Mentioned|p113|||||||||
13635|Myally Subgroup|38237|6|Mentioned|p132|||||||||
13635|Myally Subgroup|38276|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|38350|6|Mentioned|p10|||||||||
13635|Myally Subgroup|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|38560|6|Mentioned|p113|||||||||
13635|Myally Subgroup|38919|6|Mentioned|p494|||||||||
13635|Myally Subgroup|39362|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|39445|5|Briefly described|p35|||See also p40 and Table 2.||||||13-NOV-06
13635|Myally Subgroup|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Haslingden Group.  Includes: Alsace Quartzite, Bortala Fm., Whitworth Quartzite and Lochness Formation.||||||15-JUN-06
13635|Myally Subgroup|39622|6|Mentioned|p21|||||||||
13635|Myally Subgroup|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
13635|Myally Subgroup|39925|6|Mentioned|Fig.9|||||||||
13635|Myally Subgroup|39934|6|Mentioned|Fig.3|||||||||
13635|Myally Subgroup|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13635|Myally Subgroup|40202|6|Mentioned|p719|||||||||
13635|Myally Subgroup|40221|3|Fully described|p8|||||||||
13635|Myally Subgroup|40394|6|Mentioned|p284|||||||||
13635|Myally Subgroup|40598|6|Mentioned|Fig.1|||||||||
13635|Myally Subgroup|40623|5|Briefly described|p98|||||||||
13635|Myally Subgroup|40840|6|Mentioned|Map legend|||||||||
13635|Myally Subgroup|41277|6|Mentioned|p83|||||||||
13635|Myally Subgroup|41298|6|Mentioned|Map legend|Carpentarian||||||||
13635|Myally Subgroup|41307|4|Described|p9|||||||||
13635|Myally Subgroup|41978|6|Mentioned|p501|||||||||
13635|Myally Subgroup|41979|6|Mentioned|Fig.2 P512|||||||||
13635|Myally Subgroup|42234|5|Briefly described|p1056|||||||||
13635|Myally Subgroup|42367|6|Mentioned|p17|||Part of Haslingden Group||||||
13635|Myally Subgroup|42503|6|Mentioned|p336|||||||||
13635|Myally Subgroup|42523|5|Briefly described|p372|||||||||
13635|Myally Subgroup|42565|5|Briefly described|Table 1 P5, P2|||||||||
13635|Myally Subgroup|42676|5|Briefly described|Fig.2 P41|||||||||
13635|Myally Subgroup|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Upper part of the Haslingden Group.||||||09-FEB-09
13635|Myally Subgroup|42782|5|Briefly described|p458|||||||||
13635|Myally Subgroup|42818|4|Described|p211, Table 1 p208|||Of the Haslingden Group.||||||13-NOV-06
13635|Myally Subgroup|43608|6|Mentioned|Fig.11,p11|||||||||
13635|Myally Subgroup|43616|6|Mentioned|p3|||||||||
13635|Myally Subgroup|43760|5|Briefly described|p431|||||||||
13635|Myally Subgroup|43788|6|Mentioned|p20|||||||||
13635|Myally Subgroup|43928|6|Mentioned|23|||||||||
13635|Myally Subgroup|44195|6|Mentioned|p356 Fig.9|||||||||
13635|Myally Subgroup|45136|4|Described|Table 1|||||||||
13635|Myally Subgroup|45161|6|Mentioned|p12|||||||||
13635|Myally Subgroup|45166|4|Described|p16|||||||||
13635|Myally Subgroup|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
13635|Myally Subgroup|46960|6|Mentioned|p215|||||||||
13635|Myally Subgroup|46962|4|Described|Table 1|||See also Fig.3.||||||
13635|Myally Subgroup|46995|5|Briefly described|p268|||||||||
13635|Myally Subgroup|46996|6|Mentioned|p273|||||||||
13635|Myally Subgroup|47083|4|Described|p6-10||Proterozoic|Of Haslingden Group. Overlain by Quilalar Fm - conformable. Underlain by Eastern Creek Volcanics.||||||13-NOV-06
13635|Myally Subgroup|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Haslingden Group.  Unconformably overlies the Leichhardt Volcanics; conformably overlies the Eastern Creek Volcanics.||||||
13635|Myally Subgroup|50332|5|Briefly described|p17, p70|Proterozoic|Proterozoic|Includes; Alsace Quartzite, Bortala Formation, Whitworth Quartzite and Lochness Formation. Conformably overlies Eastern Creek Volcanics. Consists of feldspathic and quartz sandstones, with minor dolomitic and calcareous beds and felsic volcanics.||||||07-FEB-11
13635|Myally Subgroup|50536|6|Mentioned|p8.4|||Geological Province: Mount Isa Inlier. Intruded by Sybella Suite.||||||
13635|Myally Subgroup|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1756 Ma, 1742 Ma. Conformably overlies Eastern Creek Volcanics. Geological Province: Western Fold Belt.||||||19-DEC-07
13635|Myally Subgroup|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|Of the Haslingden Group.||||||07-NOV-08
13635|Myally Subgroup|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
13635|Myally Subgroup|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: >1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
13635|Myally Subgroup|61922|5|Briefly described|p8, p9 Fig. 3|||An immature ferruginous quartz arenite. Discordantly overlies the Eastern Creek Volcanics. Geological Province: Mount Isa Inlier/Western Fold Belt.  See also p19 Fig.11,  p21 Fig.13..||||||
13635|Myally Subgroup|61923|5|Briefly described|p29 Fig.2, p30|||Upper section of the Haslingden Group. Generally a sandstone series consisting of either mature, silica-cemented white quartzite or immature, orange weathering ferruginous sandstone. Geological Province: Mount Isa Inlier.||||||
13635|Myally Subgroup|61929|5|Briefly described|p128 Fig. 2|||Includes Alsace Quartzite, Bortala Formation and Whitworth Quartzite.||||||
13635|Myally Subgroup|61936|5|Briefly described|p193|||Overlies Eastern Creek Volcanics; overlain by Quilalar Formation. Geological Province: Leichhardt Superbasin, Western Fold Belt, Mount Isa Inlier.||||||
13635|Myally Subgroup|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin.||||||
13635|Myally Subgroup|62288|5|Briefly described|p122 Fig. 2, p34|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Myally Supersequence spanning the interval ~1780-1765Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
13635|Myally Subgroup|63023|5|Briefly described|p1025 Fig. 2|||Geological Province: Leichhardt Superbasin.||||||22-JUL-13
13635|Myally Subgroup|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Includes; Alsace Quartzite, Bortalla Formation, Whitworth Quartzite, Lochness Formation. Overlain by Quilalar Formation, underlain by Mount Guide Quartzite. Thickness: 4000m. Geological Province: Leichhardt Superbasin.||||||07-FEB-11
13635|Myally Subgroup|63113|5|Briefly described|p1214 Fig.2.||||||Includes the Whitworth Quartzite; Lochness, Quilalar, Fiery Creek and Surprise Creek Formations.|||
13635|Myally Subgroup|63114|5|Briefly described|p1253 Fig.2. |||Leichhardt superbasin.|||Includes the Lochness Formation, Whitworth Quartzite, Bortala Formation and Alsace Quartzite.|Overlies Eastern Creek Volcanics. Is overlain by Quilalar Formation.||
13635|Myally Subgroup|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. 4000 m thick.|||||Mainly sandstone, minor siltstone.|
13635|Myally Subgroup|63884|5|Briefly described|p14|||Siliciclastic; quartzite, sandstone and siltstone.||||||
13635|Myally Subgroup|64250|5|Briefly described|p11 fig 3, p19, p22, p23, p27|||Western Fold Belt, Mount Isa Inlier. Forms a single Supersequence with the Eastern Creek Volcanics.|1773 +/- 2 Ma|Haslingden Group||||
13635|Myally Subgroup|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Topmost rocks of Eastern Creek Volcanics. Age: ca.1775Ma.||||||07-FEB-11
13635|Myally Subgroup|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
13635|Myally Subgroup|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of the Haslingden Group. Age: ca.1775Ma. Geological Province: Mt Isa Inlier. Consists of quartz-feldspathic sandstones.||||||07-FEB-11
13635|Myally Subgroup|64834|5|Briefly described|p13 Fig.2, p31-32|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.|||Lochness Formation, Whitworth Formation, Bortalla Formation, Alsace Quartzite|||
13635|Myally Subgroup|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Leichhardt River Fault Trough.||Unit in Haslingden Group.||||
13635|Myally Subgroup|65396|6|Mentioned|p16, p82, p175, p187, p190, p193-194|Statherian|Statherian|See also p196, p241. Leichhardt Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough. Predominantly continental to shallow restricted marine deposits.|1773 +/- 2 Ma (Neumann et al., 2005).|Haslingden Group||Overlies Eastern Creek Volcanics; overlain by Quilalar Formation.||
13635|Myally Subgroup|65505|6|Mentioned|979, Fig 9|Proterozoic|Proterozoic|||||||
13635|Myally Subgroup|66529|5|Briefly described|p32, p34 |||Leichhardt Superbasin.||||Overlies Eastern Creek Volcanics.|Coarse-to-medium-grained siliciclastics.|
13635|Myally Subgroup|66824|6|Mentioned|p135|||||||||
13635|Myally Subgroup|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||Unit in Haslingden Group.||||
13635|Myally Subgroup|67323|4|Described|p11-12, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Widespread throughout the Mount Isa Inlier.|Deposition ~1775-1760 Ma.|Haslingden Group.|Includes Alsace Quartzite, Bortala Formation, Lochness Formation, Whitworth Quartzite.|Unconformably overlain by Surprise Creek Formation. Geophysics suggests may be underlain by Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|67499|5|Briefly described|p938|||Of Derrick (1982), Blake and Stewart (1992). See also Myally Group, Fig. 3.||Of the Haslingden Group.||Underlain by the Eastern Creek Volcanics.||
13635|Myally Subgroup|67539|6|Mentioned|p2|||Includes sandstones. Shown as Myally Sub Group in Fig. 3, p4. Previously considered to unconformably overlie Ewen Granite.||||Intruded by Ewen Granite.||
13635|Myally Subgroup|68020|6|Mentioned|p126||||||Includes Whitworth Quartzite.|||
13635|Myally Subgroup|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Part of Myally Supersequence, Leichhardt Superbasin, Western Succession.||||Overlies Eastern Creek Volcanics, unconformably overlain by Quilalar Formation. Part equivalent to Marraba Volcanics?||
13635|Myally Subgroup|68542|6|Mentioned|p12|||||||||
13635|Myally Subgroup|68575|6|Mentioned|p1, p37, p78, p112, p124|||A 500m thick sandstone sequence, between Argylla Formation and overlying Ballara Quartzite, may be an equivalent of this unit.||||||
13635|Myally Subgroup|68576|5|Briefly described|Q_2: p12|||Western Succession, Mount Isa region.||||Is overlain by Mary Kathleen Group (equivalents).||
13635|Myally Subgroup|69056|6|Mentioned|p2 |||||||||
13635|Myally Subgroup|69222|5|Briefly described|p221, p222 Fig.2|||Leichhardt River Fault Trough. Post-rift subsidence deposits.|||Includes Pickwick Metabasalt, Alsace Quartzite, Bortala Formation, Whitworth Quartzite|Overlies Eastern Creek Volcanics, overlain by Quilalar Formation||09-FEB-18
13635|Myally Subgroup|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||Unit in Haslingden Group.||Is overlain by Quilalar Formation.||25-JAN-19
13635|Myally Subgroup|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||||||
13635|Myally Subgroup|69591|4|Described|p33, p38, p45-46, p49, p57, p88, p105|||Leichhardt Superbasin. Probably absent N of the Murphy Tectonic Ridge. Part of Myally Supersequence. E-W-trending normal faults (from north-south extension) were active during deposition.|~1773 Ma (Neumann et al., 2006).|Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics. Is overlain unconformably by Gunpowder Creek Formation. Is faulted against Mount Isa Group.|Siliciclastic sediments.|
13635|Myally Subgroup|70282|5|Briefly described|p544 table 1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||Overlies Eastern Creek Volcanics.|Clastic sediments and carbonates.|13-FEB-18
13635|Myally Subgroup|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Haslingden Group.|Alsace, Whitworth Quartzites; Bortala, Lochness Formations.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform and Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Bigie Formation and Quilalar Formation. Underlain by Eastern Creek Volcanics and Haslingden Group.||
13635|Myally Subgroup|71799|5|Briefly described|p150 fig 2, p153 tbl 1, p153|Statherian|Statherian|Lawn Hill. Source of age not provided. Referred to as the Myally Supersequence on p153 and also Myally Supergroup.|1773 +/- 3 Ma (SHRIMP)||Includes the Alsace Quartzite.|Overlies the Eastern Creek Volcanics. Overlain by the Quilalar Formation.||
13635|Myally Subgroup|71960|6|Mentioned|p77, 86|||Provenance shown to be from west.||Of Haslingden Group.||||
13635|Myally Subgroup|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Haslingden Group|Includes Alsace Quartzite, Bortala Formation, Whitworth Quartzite.|Overlies Eastern Creek Volcanics.||
13635|Myally Subgroup|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province. Age given as U-Pb zircon sedimentary depositional age. [material dated not stated]|1773 +/-2 Ma||Whitworth Quartzite, Lochness Formation, Bortala Formation and Alsace Quartzite|Overlies Eastern Creek and shown as partially underlying Quilarlar Formation and Don Creek Sandstone.||
13635|Myally Subgroup|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group||Overlies Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain.||Haslingden Group||Overlies Eastern Creek Volcanics.|Variably feldspathic and lithic sandstone, siltstone and minor conglomerate.|
13635|Myally Subgroup|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province. U-Pb zircon sedimentary depositional age given [but no indication of what unit dated, or where the sample sits stratigraphically].|1773 +/- 2 Ma||Whitworth Quartzite, Lochness Formation, Bortala Formation and Alsace Quartzite.|Shown as underlying Carrara Range Group.||
13635|Myally Subgroup|72919|5|Briefly described|p56, p63-64|||Mount Isa Province. Previously Myally beds.||Myally Supersequence|Alsace Quartzite, Bortala Formation, Whitworth Quartzite, Lochness Formation|||
13635|Myally Subgroup|73042|6|Mentioned|p4|Statherian|Statherian|Mount Isa Province, Leichhardt Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1773 +/- 2 Ma (see Fig.1.2)||Whitworth Quartzite, Lochness Formation, Bortala Formation, Alsace Quartzite.|Underlain by Eastern Creek Volcanics. Partly overlain(?) by Quilalar Formation.||
13635|Myally Subgroup|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13, p20|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1768+/-8 Ma, 1773+/-2 Ma maximum depositional ages||||Clastics.|
13654|Myrtle Creek Sandstone|9194|5|Briefly described|Map legend|Jurassic|Jurassic|Orthoquartzite and quartzose sandstone, minor silty mudstone.  Overlies the Brooweena Formation; overlain by Graham's Creek Formation.||||||12-JUL-04
13654|Myrtle Creek Sandstone|22845|6|Mentioned|Fig6|Jurassic|Triassic|||||||
13654|Myrtle Creek Sandstone|22846|6|Mentioned|Plate 1|Jurassic|Late Triassic|||||||
13654|Myrtle Creek Sandstone|23190|6|Mentioned|Fig10p16|||||||||
13654|Myrtle Creek Sandstone|23251|5|Briefly described|Table 1 p8, p6||Rhaetian|Age based on estimation of miospores. Geological Province: Maryborough Basin. Max. thickness 300 m. See also the informal Myrtle Creek sandstone.||||||13-NOV-06
13654|Myrtle Creek Sandstone|23841|4|Described|p448|Jurassic|Jurassic|Of Woogaroo Sub-Group. Geological Province: Maryborough Basin.  Maximum thickness: 455m.||||||14-AUG-08
13654|Myrtle Creek Sandstone|24382|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Duckinwilla Group.||||||13-NOV-06
13654|Myrtle Creek Sandstone|29651|6|Mentioned|Table 1|||||||||
13654|Myrtle Creek Sandstone|30654|4|Described|p49|||See also p50,53,55,56,59. Jurassic age.||||||13-NOV-06
13654|Myrtle Creek Sandstone|30655|3|Fully described|p19|||See also Table 1||||||
13654|Myrtle Creek Sandstone|30914|6|Mentioned|Map legend|Jurassic|Triassic|Triassic - Jurassic||||||
13654|Myrtle Creek Sandstone|32137|6|Mentioned|p355|||||||||
13654|Myrtle Creek Sandstone|32774|5|Briefly described|Table 2|||||||||
13654|Myrtle Creek Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic||||||
13654|Myrtle Creek Sandstone|35101|3|Fully described|p49|||||||||
13654|Myrtle Creek Sandstone|35813|6|Mentioned|p574|||||||||
13654|Myrtle Creek Sandstone|35866|6|Mentioned|p410|||||||||
13654|Myrtle Creek Sandstone|36101|6|Mentioned|p171|||||||||
13654|Myrtle Creek Sandstone|36575|6|Mentioned|Fig.1|||||||||
13654|Myrtle Creek Sandstone|36926|6|Mentioned|p165|||||||||
13654|Myrtle Creek Sandstone|37118|6|Mentioned|p317|||||||||
13654|Myrtle Creek Sandstone|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
13654|Myrtle Creek Sandstone|37618|4|Described|p19|||||||||
13654|Myrtle Creek Sandstone|37861|6|Mentioned|p591|||||||||
13654|Myrtle Creek Sandstone|38397|4|Described|Table 2|||||||||
13654|Myrtle Creek Sandstone|38402|6|Mentioned|p72|||||||||
13654|Myrtle Creek Sandstone|39315|6|Mentioned|Fig.5|||||||||
13654|Myrtle Creek Sandstone|39445|5|Briefly described|Table 10|||||||||
13654|Myrtle Creek Sandstone|39505|6|Mentioned|p191|||||||||
13654|Myrtle Creek Sandstone|39943|6|Mentioned|Table 11A|||||||||
13654|Myrtle Creek Sandstone|40051|4|Described|p10|||||||||
13654|Myrtle Creek Sandstone|40623|5|Briefly described|p54|||||||||
13654|Myrtle Creek Sandstone|41736|6|Mentioned|p120|||||||||
13654|Myrtle Creek Sandstone|41738|5|Briefly described|p173|||||||||
13654|Myrtle Creek Sandstone|41778|6|Mentioned|p376|||||||||
13654|Myrtle Creek Sandstone|41916|6|Mentioned|p522|||||||||
13654|Myrtle Creek Sandstone|41917|6|Mentioned|p531|||||||||
13654|Myrtle Creek Sandstone|42282|4|Described|p3|Early Jurassic|Late Triassic|||||||
13654|Myrtle Creek Sandstone|42450|5|Briefly described|p407|||||||||
13654|Myrtle Creek Sandstone|42616|4|Described|p6|||||||||
13654|Myrtle Creek Sandstone|42636|6|Mentioned|p8|||||||||
13654|Myrtle Creek Sandstone|42695|5|Briefly described|Fig.2|Triassic||||||||
13654|Myrtle Creek Sandstone|42751|3|Fully described|p27|||||||||
13654|Myrtle Creek Sandstone|42764|4|Described|p27|||||||||
13654|Myrtle Creek Sandstone|42801|6|Mentioned|Fig.2 P82|||||||||
13654|Myrtle Creek Sandstone|42894|3|Fully described|p21|||See also Fig.2 p22.||||||13-NOV-06
13654|Myrtle Creek Sandstone|43008|5|Briefly described|map legend|||||||||
13654|Myrtle Creek Sandstone|43059|6|Mentioned|p9|||Of the Duckinwilla Group.||||||13-NOV-06
13654|Myrtle Creek Sandstone|43077|5|Briefly described|p8|||||||||
13654|Myrtle Creek Sandstone|43100|3|Fully described|p44||Late Triassic|Of the Duckinwilla Group.||||||13-NOV-06
13654|Myrtle Creek Sandstone|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Maryborough Basin.||||||12-APR-05
13654|Myrtle Creek Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
13654|Myrtle Creek Sandstone|43995|14|Not recorded|Tb.p10||Triassic|||||||
13654|Myrtle Creek Sandstone|44075|14|Not recorded|p251|||||||||
13654|Myrtle Creek Sandstone|44084|14|Not recorded|p32(Tb)||Early Jurassic|Maryborough Basin.||||||
13654|Myrtle Creek Sandstone|44091|14|Not recorded|p58||Lias|||||||
13654|Myrtle Creek Sandstone|44239|2|Defined|p278-9|||Overlies Brooweena Formation. Correlated with Bundamba Group.||||||
13654|Myrtle Creek Sandstone|44241|14|Not recorded|p12|||||||||
13654|Myrtle Creek Sandstone|44385|14|Not recorded|p6|||On Myrtle Creek Formation white card. (In ref. as Myrtle Creek Sand Stone)||||||
13654|Myrtle Creek Sandstone|44387|14|Not recorded|p17|||On Myrtle Creek Formation white card.||||||
13654|Myrtle Creek Sandstone|44616|14|Not recorded|p33,35,36||Jurassic|Massive orthoquartzite, fair porosity.||||||
13654|Myrtle Creek Sandstone|44750|14|Not recorded|p12,16||Jurassic|||||||
13654|Myrtle Creek Sandstone|44783|14|Not recorded|p2|||||||||
13654|Myrtle Creek Sandstone|44814|14|Not recorded|p485,486||Late Triassic|||||||
13654|Myrtle Creek Sandstone|44923|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|||||||
13654|Myrtle Creek Sandstone|44925|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
13654|Myrtle Creek Sandstone|44928|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
13654|Myrtle Creek Sandstone|45440|4|Described|p.2,14,26,27,29-88||Jurassic|Tb.1. Of many pages.||||||
13654|Myrtle Creek Sandstone|50320|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|Geological province: Nambour Basin.||||||09-JUN-04
13654|Myrtle Creek Sandstone|60077|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Sandstone, shale, siltstone, conglomerate.||||||
13654|Myrtle Creek Sandstone|60281|5|Briefly described|p36, Fig. 30 App. 1|Late Triassic|Late Triassic|Of the Duckinwilla Group.  Thick, fluvial sediments composed largely of orthoquartzite and quartzose sandstone, although lower beds comprise interbedded sandstone, siltstone and shale.  Conformably overlain by Tiaro C.M. Geol. Prov: Maryborough Basin.||||||
13654|Myrtle Creek Sandstone|61611|5|Briefly described|p264, p266, p265 Fig. 3|Early Jurassic|Late Triassic|Lateral equilalent of Precipice Sandstone. Geological Province: Maryborough Basin.||||||13-MAR-09
13654|Myrtle Creek Sandstone|62594|5|Briefly described|p546 Fig. 3|Middle Jurassic|Late Triassic|Geological Province: Maryborough Basin||||||
13654|Myrtle Creek Sandstone|63187|5|Briefly described|p106|Early Jurassic|Triassic|In the southern part of the Noosa area - intruded by silicic rocks.||||||
13654|Myrtle Creek Sandstone|63821|4|Described|p23||Late Triassic|Of the Duckinwilla Group. Overlain by Tiaro Coal Measures, either conformably or disconformably. Geological Province: Nambour Basin.Comprises quartzose sandstone of which the lower part is interbedded sandstone, siltstone and shale.||||||07-FEB-11
13654|Myrtle Creek Sandstone|64665|5|Briefly described|p53 Fig.2.|Early Jurassic|Late Triassic|Northern Nambour Basin. Correlates with Ripley Road Sandstone (Clarence-Moreton Basin) and lower part of Landsborough Sandstone (Southern Nambour Basin).||||Is overlain by Tiaro Coal Measures.||
13654|Myrtle Creek Sandstone|65452|5|Briefly described|p5-6|Early Jurassic|Late Triassic|But shown as Cretaceous on p6.||||Locally overlies Agnes Water Volcanics.|Quartzose sandstone.|
13654|Myrtle Creek Sandstone|65668|6|Mentioned|p11|Jurassic|Jurassic|Overlies Agnes Water Volcanics.||||||
13654|Myrtle Creek Sandstone|67402|5|Briefly described|p165 tbl LPB1, p234-p237|Sinemurian|Norian|Maryborough Basin. Deposited in a fluvial environment. Is one of the only potential reservoir units in the Maryborough Basin.||Duckinwilla Group||Overlain by the Tiaro Coal Measures. Equivalent to the Precipice Sandstone.|Thick quartzose sandstone.|
13654|Myrtle Creek Sandstone|68135|5|Briefly described|p52 fig 2b|Pleinsbachian|Hettangian|Northern Nambour Basin. Contains plant macrofossils.||||Is overlain by Tiaro Coal Measures.|Cross-bedded sandstone.|14-SEP-17
13654|Myrtle Creek Sandstone|68319|5|Briefly described|Map Legend|Early Jurassic|Late Triassic|Nambour Basin||||Unconformably overlain by the Maryborough Formation. Unconformably underlain by the Brooweena Formation.|Quartzose sandstone, orthoquartzite, sublabile to labile sandstone, siltstone, shale.|
13654|Myrtle Creek Sandstone|68332|5|Briefly described|Map legend.|Early Jurassic|Late Triassic|Nambour Basin.|||||Quartzose sandstone, orthoquartzite, sublabile to labile sandstone, siltstone, shale.|
13654|Myrtle Creek Sandstone|68679|6|Mentioned|p430|||||||Unconformably overlies Musket Flat Granodiorite.||
13654|Myrtle Creek Sandstone|69582|5|Briefly described|p48, p50, p53|||Nambour Basin. Thermal conductivity is provided. Intersected in GSQ Maryborough 16. Approximately 650m thick.||Duckinwilla Group||Overlain by the Tiaro Coal Measures. Unconformably overlies the Brooweena Formation.|Quartzose to sublabile sandstone with siltstone and shale.|
13654|Myrtle Creek Sandstone|69594|4|Described|p519, p546-547, p548 Fig.7.20, p560-561|Sinemurian|Rhaetian|See also p572. Northern Nambour Basin. Maximum thickness 550m (in type section); 60m in the north.||Duckinwilla Group.||Is overlain by Tiaro Coal Measures. Is intruded by Noosa Quartz Diorite and Mount Urah Granodiorite. Equivalent to Nambour Formation with Landsborough Sandstone.|Basal conglomerate with mudstone containing plant fossils; sandstone with weathered lithics; siltstone and shale. Upper part: light grey, thick-bedded, medium- to coarse-grained orthoquartzite or quartzose sandstone; silica cement dominant.|
13654|Myrtle Creek Sandstone|69599|6|Mentioned|p637|||Nambour Basin. Is intruded by Mounts Coolum, Peregian and Tinbeerwah.||||||
13654|Myrtle Creek Sandstone|72298|5|Briefly described|p802|||Clarence-Moreton Basin. Has supplied small supplies of groundwater for irrigation.||||||
13654|Myrtle Creek Sandstone|73450|6|Mentioned|p86|Jurassic|Triassic|||||Intruded by Allandale Granite.||
13654|Myrtle Creek Sandstone|73570|6|Mentioned|p914, p915 Fig.4, p916, p917 Fig.5|Early Jurassic|Early Jurassic|Nambour Basin.|||||Sandstones.|
13663|Mytton Formation|23032|4|Described|p25,29 fig6||Middle Devonian|||||||
13663|Mytton Formation|23424|4|Described|Table 8.1 p336.||Givetian|Age: Middle Devonian (Givetian); conodonts. Of Broken River Group, Graveyard Creek Subprovince. Underlying Unit Wando Vale Subgroup (c). Maximum thickness 940 m.||||||
13663|Mytton Formation|23431|5|Briefly described|p540|||||||||
13663|Mytton Formation|23522|5|Briefly described|p250 Fig 6|Frasnian|Frasnian|||||||
13663|Mytton Formation|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Frasnian|Frasnian|Of the Broken River Group. Disconformably / unconformably overlain by the Bulgeri Formation. Overlies the Papilio Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
13663|Mytton Formation|24610|5|Briefly described|p71|Frasnian|Frasnian|Parent: Broken River Group.||||||
13663|Mytton Formation|24614|5|Briefly described|p191 Fig. 1|||Of the Broken River Group. Includes the Stanley Limestone Member. Unconformably overlain by Bulgeri Formation. Geological Province: Broken River Province.||||||07-FEB-11
13663|Mytton Formation|41260|4|Described|Table 1|||Reserved as Mytton Member||||||
13663|Mytton Formation|41679|2|Defined|p260|Frasnian|Givetian|Age: late Givetian to Frasnian.||||||
13663|Mytton Formation|41719|6|Mentioned|Fig.2|||||||||
13663|Mytton Formation|41739|6|Mentioned|p301|||||||||
13663|Mytton Formation|41740|6|Mentioned|p222|||||||||
13663|Mytton Formation|42015|6|Mentioned|p318|||||||||
13663|Mytton Formation|42031|5|Briefly described|Fig.5 P762|||||||||
13663|Mytton Formation|42032|6|Mentioned|Fig.12 P505|||||||||
13663|Mytton Formation|42054|6|Mentioned|p273|||||||||
13663|Mytton Formation|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
13663|Mytton Formation|42709|6|Mentioned|map legend|||||||||
13663|Mytton Formation|42933|3|Fully described|Table 2|||See also p124||||||
13663|Mytton Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Broken River Group.||||||
13663|Mytton Formation|50093|6|Mentioned|p329 Fig.2|Frasnian|Frasnian|Of Broken River Group.||||||07-FEB-11
13663|Mytton Formation|63152|5|Briefly described|p120 Fig. 3|Frasnian|Frasnian|Of the Broken River Group. Mudstones with subordinate lithic arenites and occasional granule and pebble conglomerates.||||||10-APR-07
13663|Mytton Formation|65214|6|Mentioned|p280, p282|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
13663|Mytton Formation|68336|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Broken River Group.|Includes Stanley Limestone Member.||Mudstone and fine- to coarse-grained sublithic arenite; minor granule to pebble conglomerate, oolitic/oncolitic conglomerate and oolitic limestone.|
13663|Mytton Formation|68341|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Broken River Group.|Includes Stanley Limestone Member.||Mudstone and fine- to coarse-grained sublithic arenite; minor granule to pebble conglomerate, oolitic/oncolitic conglomerate and oolitic limestone.|
13663|Mytton Formation|68478|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Broken River Group.|Includes Stanley Limestone Member.|Conformably underlain by the Papilio Formation.|Mudstone and fine to coarse-grained sublithic arenite; minor granule to pebble conglomerate, oolitic/oncolitic conglomerate and oolitic limestone.|
13663|Mytton Formation|68479|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Broken River Group.|Includes Stanley Limestone Member.|Conformably underlain by the Papilio Formation.|Mudstone and fine to coarse-grained sublithic arenite; minor granule to pebble conglomerate, oolitic/oncolitic conglomerate and oolitic limestone.|
13663|Mytton Formation|69030|5|Briefly described|p6|Devonian|Devonian|Graveyard Creek Subprovince (Broken River Province).||Broken River Group.||||
13663|Mytton Formation|69592|3|Fully described|p259, p266-267, p272, p277, p298-299|Middle Devonian|Early Devonian|Graveyard Creek Subprovince, Broken River Province. Is 500m thick in the type section, in the Broken River, including a 100m-thick upper interval of massive mudstone with interbeds of fine-grained quartzose sandstone. Trace and bioclast fossils. Open, shallow, intertidal shelf deposits. Probably extends into early Frasnian.||Uppermost Broken River Group.|Stanley Limestone Member.|Overlies Papillio Formation. Is overlain unconformably by Rockfields Member (Bulgeri Formation). Is faulted against Broken River Group.|Mainly medium-bedded to very thick-bedded, well-sorted, fine-grained quartzose sandstone interlayered with bioturbated mudstone or thin beds of graded and ripple cross-laminated sandstone.|
13710|Nambour Formation|42893|2|Defined|p7||Late Triassic|||||||
13710|Nambour Formation|42894|5|Briefly described|Fig.1 P20|||||||||
13710|Nambour Formation|44925|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
13710|Nambour Formation|60281|6|Mentioned|p26|||Geological Province: Nambour Basin.||||||
13710|Nambour Formation|64665|5|Briefly described|p53 Fig.2.|Late Triassic|Late Triassic|Southern Nambour Basin.||Unit in Woogaroo Subgroup.||Is overlain by Landsborough Sandstone.||
13710|Nambour Formation|67402|5|Briefly described|p254, p255|Norian|Norian|Nambour Basin. Deposited in a fluvio-lacustrine environment. 50m thick.|||||Volcaniclastic conglomerate, sandstone, siltstone and shale.|
13710|Nambour Formation|69594|4|Described|p519, p546-547|Rhaetian|Rhaetian|McKellar (1993). Southern Nambour Basin. Upward-coarsening cycles predominate; clasts include volcanic rocks; alluvial fan deposits sourced from North Arm Volcanic Group. RELATED UNITS (continued): Equivalent to Aberdare Conglomerate with Raceview Formation; also to Moorooka Formation and basal Landsborough Sandstone; part-equivalent to Myrtle Creek Sandstone.||Woogaroo Subgroup.||Unconformably overlies North Arm Volcanic Group. Is overlain by Landsborough Sandstone. See COMMENTS for equivalent units.|In type section: dark grey to black, rudaceous, arenaceous and argillaceous volcaniclastics, fine-grained carbonaceous shales and thin coal seams. Elsewhere: matrix-supported conglomerates commonly overlie grain-supported ones.|
13738|Namur Sandstone|13497|3|Fully described|p26, p115, p115 fig 6.33|Jurassic|Jurassic|Eromanga Basin. Deposited in a low sinuosity fluvial environment. See also p138 fig 8.17, p139 fig 8.18, p141, p146, p151 fig 9.23, p152 fig 9.25,  p171, p173, p184, p216. Incorrectly referred to as the obsolete Namur Sandstone Member in the App, p216.||||Overlies the Adori Sandstone and the Westbourne Formation. Overlain by the McKinlay Member, Murta Formation and the Cadna-owie Formation.|Sandstone.|
13738|Namur Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Late Jurassic|In Eromanga Basin.||||||
13738|Namur Sandstone|22839|6|Mentioned|P33|||||||||
13738|Namur Sandstone|22883|5|Briefly described|P31, Fig2||Late Jurassic|Overlying unit is Murta Formation, underlying unit is Birkhead Formation.||||||16-SEP-08
13738|Namur Sandstone|22909|5|Briefly described|42|||||||||
13738|Namur Sandstone|23054|6|Mentioned|Fig5p22|||||||||
13738|Namur Sandstone|23155|2|Defined|p26-27 & Fig 15 p28|Early Cretaceous|Late Jurassic|For Max. Thickness of type section see Fig 15 on p28.  For location of type section and details of previous names see p27.||||||16-APR-08
13738|Namur Sandstone|23375|4|Described|Fig2 p265,268-271|Berriasian|Oxfordian|Laterally equivalent to lower-middle Hooray Sandstone, Westbourne Formation and Adori Sandstone. IN the Eromanga Basin.||||||17-JAN-08
13738|Namur Sandstone|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13738|Namur Sandstone|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|37287|6|Mentioned|p33|||||||||
13738|Namur Sandstone|38108|6|Mentioned|Table 1|||||||||
13738|Namur Sandstone|38730|6|Mentioned|p29|||||||||
13738|Namur Sandstone|40030|6|Mentioned|p131|||||||||
13738|Namur Sandstone|40670|6|Mentioned|p213|||||||||
13738|Namur Sandstone|41061|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41099|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41123|6|Mentioned|p180|||||||||
13738|Namur Sandstone|41216|6|Mentioned|p300|||||||||
13738|Namur Sandstone|41705|6|Mentioned|p122|||||||||
13738|Namur Sandstone|41712|6|Mentioned|p282|||||||||
13738|Namur Sandstone|41724|6|Mentioned|p382|||||||||
13738|Namur Sandstone|42357|6|Mentioned|p11|||||||||
13738|Namur Sandstone|43711|6|Mentioned|p18|||||||||
13738|Namur Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Birkhead Formation; overlain by Murta Formation; lateral to Adori Sandstone, and possibly to Algebuckina Sandstone also. Geological Province: Eromanga  Basin.||||||31-JAN-08
13738|Namur Sandstone|61613|6|Mentioned|p282, p284|Jurassic|Jurassic|||||||07-FEB-11
13738|Namur Sandstone|61614|6|Mentioned|p295, p290 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
13738|Namur Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|62028|6|Mentioned|p10|||Abbreviation? of Namur Sandstone Member.||||||26-FEB-08
13738|Namur Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
13738|Namur Sandstone|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale and Cadna-owie Formation.||
13738|Namur Sandstone|63979|5|Briefly described|Fig. 44|Berriasian|Oxford|Supersedes "Namur Sandstone member". As a formally defined SA unit, this encompasses the Queensland interval Adori Sandstone-Westbourne Formation-Hooray Sandstone.||||||07-FEB-11
13738|Namur Sandstone|64048|6|Mentioned|p71|||Superseded "Namur Sandstone Member" of the Mooga Formation in South Australia. Mooga Formation now obsolete. Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|64197|6|Mentioned|p630 Fig.6|Late Jurassic|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Member.||
13738|Namur Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Formation.||
13738|Namur Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
13738|Namur Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Late Jurassic|Of Eromanga Basin. Overlain by Murta Formation. Unit shown to include unconformity around Jurassic-Cretaceous boundary? Quartz-rich sediment. See also "upper Namur Sandstone".||||||08-MAR-12
13738|Namur Sandstone|65489|5|Briefly described|p11, p15, p17, p47, p49, p61, p73, p96|Early Cretaceous|Jurassic|See also p154-155, p158-160. Eromanga Basin. Fair to excellent reservoir quality. Predominantly anticlinal traps. Gas and oil reservoir accounting for 30% and 15% respectively of the Basin's production.||||Overlies Westbourne Formation. Is overlain by Murta Formation.|Braided fluvial sandstone.|
13738|Namur Sandstone|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded and quartzose sandstone; minor siltstone and mudstone.|
13738|Namur Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Injune Creek Group. Is overlain by Murta Formation.||
13738|Namur Sandstone|66623|3|Fully described|p34, p102, pp238-249. |Cretaceous|Cretaceous|Name introduced by Mount (1981) as member of Mooga Formation; formation status by Gravestock et al. (1995). Partly equivalent to Gum Vale Beds (Rose and Brunker 1969) and Warratta Sandstone Member (Moreton 1982). Equivalent to lower part of Hooray Sandstone and Algebuckina Sandstone in Queensland. Overall, an upward-fining sequence. Variably ferruginised and cross-bedded. Thickness varies to 1200 m. Basal section hosts flaky alluvial gold and nuggets. Silicified wood locally abundant.||||Unconformably overlies Nundora and Depot Glen Formations, as well as Tibooburra Granodiorite. Is overlain by Cadna-owie Formation and, locally, by Eyre Formation and Cordillo Silcrete.|Basal quartz pebble conglomerate; non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone; minor thin claystone lenses.|
13738|Namur Sandstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga Basin. In Fig.3 also shows "upper Namur Sandstone".||||||
13738|Namur Sandstone|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous sandstone and conglomerate is mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate.|
13738|Namur Sandstone|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous and  weathered units are mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate; deeply weathered, kaolinised sandstone and claystone.|
13738|Namur Sandstone|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Easter Monday Formation of the Warratta Group. Is overlain by Wyandra Sandstone Member of Cadna-owie Formation.|Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67402|6|Mentioned|p109 tbl ERO1|||||||Equivalent to the Hooray Sandstone and Murta Formation.||
13738|Namur Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Eromanga Basin. Subsurface only. Is replaced by Algebuckina Sandstone as it pinches out at Eromanga Basin margin. Sandy lacustrine and braided river deposits.||||Overlies Birkhead Formation. Is overlain by Murta Formation.|White, fine- to coarse-grained sandstone, flat to cross-bedded, locally with calcareous cement, channel lag conglomerate; siltstone interbeds, especially in middle part; minor mudstone and coal stringers.|
13738|Namur Sandstone|68135|5|Briefly described|p52 Fig.2b|Early Cretaceous|Tithonian|Eromanga Basin.||||Unconformably overlies Westbourne Formation.|Predominantly sandstone.|
13738|Namur Sandstone|68731|6|Mentioned|pp209-211|||||||||
13738|Namur Sandstone|69001|6|Mentioned|p16|||See also Namur sandstone. Interpretations by the NSW DPI of the Namur Sandstone flanking many of the inliers are broadly grouped in this study within the Algebuckina Sandstone and equivalent units.||||||
13738|Namur Sandstone|69019|5|Briefly described|p85 Fig.21.|Early Cretaceous|Early Cretaceous|Southern Eromanga Basin.||||Overlies Westbourne Formation. Is overlain by Murta Formation.||
13738|Namur Sandstone|69023|4|Described|p79, p89 Fig.20, p91, p191-192|Hauterivian|Berriasian|Named after Delhi Petroleum exploration well Namur 1 (Mount, 1981) as Namur Sandstone Member of Mooga Formation (Nugent, 1969). This last name has been abandoned (Gravestock et al.,1995) as the Namur Sandstone Member was elevated to Formation status (Callen et al.,1994; Gravestock et al.,1995; after Martin (1983). Eromanga Basin. Thickness from ~120 to ~194m, thinning to W. Stratigraphic wells intersection data.||||Overlies Birkhead Formation. Intertongues with Westbourne Formation. Passes laterally into Algebuckina Sandstone. Is overlain by Murta Formation.|White to pale grey, flat and cross-bedded, fine- to coarse-grained, quartzose sandstone; minor siltstone and mudstone interbeds; channel lag conglomerates. Locally strongly cemented with calcite.|
13738|Namur Sandstone|69454|6|Mentioned|p38:13|||Cooper Basin. With the overlying Murta Formation, is equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13738|Namur Sandstone|69457|6|Mentioned|p41:3-4, 7|||Eromanga Basin.||||Is overlain by Murta Formation.||12-JUL-16
13738|Namur Sandstone|69594|5|Briefly described|p519, p525-527, p532, p573|Tithonian|Tithonian|Eromanga Basin. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated and the succession is called the Namur Sandstone. In QLD, where differentiation is possible, the Westbourne Formation is overlain by the Hooray Sandstone, equivalent to the topmost, Murta Formation overlying the rest of the upper part of the Namur Sandstone. This unit separating Westbourne and Murta Formations is referred to in QLD as the [informally named] upper Namur Sandstone, echoing the obsolete Namur Sandstone Member (Gray et al. 2002). A significant hydrocarbon reservoir.||||?Overlies Birkhead and Westbourne Formations unconformably. Passes laterally into Westbourne Formation locally. Is overlain by Murta Formation.||
13738|Namur Sandstone|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Westbourne Formation, overlain by McKinlay Member, Murta Formation||
13738|Namur Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Eromanga Basin.||||||
13738|Namur Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous||Age: Late Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
13738|Namur Sandstone|69946|3|Fully described|p11, p15-17, p57-58, p61, p83-85|Early Cretaceous|Late Jurassic|Originally Mooga Formation (Nugent, 1969) or part of Hooray Sandstone; named Namur Sandstone Member by Mount (1981) after Namur 1; elevated to Formation status by Gravestock et al. (1995) with the name Mooga Formation discarded in SA. In Qld the lower part of Hooray Sandstone is an equivalent. Type section is the interval 1435.22 - 1643.48m in Strzelecki 4. Generally 40 - 240m thick. Wireline log correlations.||||Conformably overlies Birkhead and Westbourne Formations. Intertongues with overlying Murta Formation or McKinlay Member. Lateral equivalent of Algebuckina Sandstone.|White to pale grey, fine- to coarse-grained sandstone with minor interbedded siltstone and mudstone; conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts; locally strongly cemented by diagenetic calcite.|
13738|Namur Sandstone|69947|5|Briefly described|p3, p7-8, p13 Fig.7.2, p27 Fig.7.16|Early Cretaceous|Late Jurassic|See also p29 Fig.7.18. Eromanga Basin. Lowstand braided fluvial sandstones form significant hydrocarbon reservoirs. Generalised stratigraphic section.||||Conformably overlies Birkhead Formation. Intertongues with Westbourne Formation. Is overlain transitionally by McKinlay Member (Murta Formation). ?Correlates with Hooray Sandstone.|Fluvial sandstones, minor shale.|
13738|Namur Sandstone|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Is overlain by Murta Formation.||
13738|Namur Sandstone|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group?|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|16-SEP-15
13738|Namur Sandstone|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. 2 un-named units: Clast supported conglomerate variant. Strongly silicified variant.|
13738|Namur Sandstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Un-named units: Ferruginous sandstone, conglomerate. Deeply weathered, leached and kaolinised sandstone and claystone.|||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. Un-named unit is a strongly silicified variant.|
13738|Namur Sandstone|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70821|5|Briefly described|p21 Fig.2.6, p31|Early Cretaceous|Jurassic|Eromanga Basin. Previously part of the [obsolete] "Lower Hooray Sandstone". 29 m thick interval, between 439-468 m in Weilmoringle 1 well.|||Appears to include the Murta Member.|Overlies Westbourne Formation. Is overlain by Cadna-owie Formation, Murta Formation..||02-DEC-16
13738|Namur Sandstone|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Late Jurassic|Eromanga Basin.  Up to 210m thick. Deposited in a braided fluvial with intertonguing lacustrine environment.||||Intertongues with the Hutton Sandstone. Overlies the Westbourne Formation. Overlain by the Murta Formation.||
13738|Namur Sandstone|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13738|Namur Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
13738|Namur Sandstone|71342|3|Fully described|Ch 1 p3, Ch 1 p6|Berriasian|Late Jurassic|Eromanga Basin. Mount (1981) named the Namur Sandstone Member after Namur 1. The unit was previously referred to as the Mooga Formation or Hooray Sandstone. Martin (1983), Gravestock et al. (1995) elevated the Namur Sandstone Member of the Mooga Formation to formation status and discarded the Mooga Formation in South Australia. Source of the majority of gas production in the Eromanga Basin. Equivalent to the lower part of the Hooray Sandstone. In Queensland this unit may be subdivided into the Adori Sandstone, Westbourne Formation and Namur Sandstone. A type section in Strzelecki 4 is given (Gravestock et al., 1995). This unit is generally 40 to 240m thick in the Cooper region. Interpreted to have been deposited in a low-sinuosity fluvial environment similar to that of the Algebuckina and Hutton Sandstones. Spore-pollen zone is given in Ch5 p57. Seal and reservoir characteristics discussed in Ch11.  Laterally equivalent to the Algebuckina Sandstone. See also Ch 1 p19, Ch3 p17-p18, Ch4 p9, Ch5 p12, Ch5 p14-p17, Ch5 p32, Ch5 p57-p58, Ch5 p82-p84, Ch6 p5-p7, Ch7 p7-p8, Ch7 p10, Ch7 p13, Ch7 p29, Ch8 p3, Ch8 p10, Ch8 p17, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p6-p8, Ch10 p14, Ch10 p18-p20, Ch11 p3-p5, Ch11 p7-p8, Ch11 p16, Ch12 p2, Ch12 p5-p6, Ch12 p15, Ch13 p2-p7, Ch13 p9-p10, Ch13 p18, Ch13 p21-p22, Ch13 p26-p27, Ch13 p29, Ch13 p31, Ch14 p3, Ch14 p5-p7.||||Conformably overlies the Birkhead Formation. Overlain by the Cadna-owie Formation. Intertongues with or is overlain by the Westbourne Formation (lower) and the Murta Formation or McKinlay Member.|White to pale grey, fine to coarse-grained sandstone with minor interbedded siltstone and mudstone. Conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts and carbonised plant fragments.|
13738|Namur Sandstone|71415|5|Briefly described|p11-14|Cretaceous|Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Probably Cretaceous in age (Exon and Senior 1976; Hill et al. 2008). LA-ICPMS zircon age populations show peaks at c. 575, c. 510, 480+\-12 and 430+\-6 Ma. Also includes small Proterozoic zircon populations at c. 2020-900 Ma, and minor Archean c. 3330 to 2555 Ma populations.||||Overlain by Cadna-owie Formation. Laterally equivalent to Algebuckina Sandstone.||19-AUG-19
13738|Namur Sandstone|71863|6|Mentioned|p5|Valanginian|Tithonian|Eromanga Basin.||||Overlain by the Murta Formation.||
13738|Namur Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Murta FZ.||
13738|Namur Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown with Hooray Sandstone as located in the Eromanga Basin.||||Unconformably overlies Westbourne Formation.||
13738|Namur Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
13738|Namur Sandstone|73251|6|Mentioned|p49, p55-56, p62|Cretaceous|Late Jurassic|Eromanga Basin. Contains hydrocarbon accumulations to which the Murta Formation contributed.||||Underlain by Birkhead and Westbourne formations. Equivalent to Westbourne Formation, Adori Sandstone and Algebuckina Sandstone. Overlain by and equivalent to McKinlay Member (Murta Formation).||
13738|Namur Sandstone|73343|6|Mentioned|p337|Cretaceous|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Mooga Formation. Overlain by Cadna-owie Formation. Equivalent to Murta Member, Hooray Sandstone, and Westbourne Formation.||
13738|Namur Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p164, p179|Cretaceous|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 152-140 Ma|||Overlies Mooga Formation, underlies Cadna-owie Formation||
13823|Nappamerri Group|13497|4|Described|iv, v, x, xi, xii, p63-p65, p69 fig 6.1|Late Triassic|Late Permian|Cooper Basin. Maximum thickness of 600m. Previously the Nappamerri Formation before being elevated to Group status by Channon and Wood (1989) and Powis (1989). Widespread and best developed in the Nappamerri and Patchawarra troughs where it is over 500m thick. See also p70, p104, p132 tbl 8.1, p133, p141, p144 fig 9.2, p146, p148-p153, p170, p189, p204, p216.|||Includes the Arrabury Formation, Tinchoo Formation and the Cuddapan Formation.|Conformably overlies the Toolachee Formation and the Gidgealpa Group.||
13823|Nappamerri Group|13516|6|Mentioned|p147 fig 5, p163, p171 fig 12|Triassic|Late Permian|From Cooper Basin||||||
13823|Nappamerri Group|22883|6|Mentioned|P31|Middle Triassic|Late Permian|||||||
13823|Nappamerri Group|23154|6|Mentioned|Map Legend|Triassic|Permian|Geological Province - Cooper Basin.||||||
13823|Nappamerri Group|23155|4|Described|p23|Triassic|Late Permian|Underlying unit on STRZELECKI - Gidgealpa Group (disconformity).||||||
13823|Nappamerri Group|23340|5|Briefly described|12|Triassic|Triassic|||||||
13823|Nappamerri Group|23375|6|Mentioned|p293, 294|||In the Cooper Basin..||||||20-NOV-06
13823|Nappamerri Group|23731|5|Briefly described|p71|Triassic|Triassic|Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13823|Nappamerri Group|24092|5|Briefly described|p8 Fig.3|||||||||17-JAN-08
13823|Nappamerri Group|24204|5|Briefly described|p262, 270|||Equivalent to Walkandi Group. Geological Province: Cooper Basin.||||||17-DEC-04
13823|Nappamerri Group|24210|5|Briefly described|p133 Fig. 2|Middle Triassic|Late Permian|Overlies the Toolachee Formation.  Geological Province: Cooper Basin.  See also p132.||||||
13823|Nappamerri Group|42008|1|Redefined|p269|Carnian|Tatarian|See also Fig.2, Fig.3, Fig.4||||||
13823|Nappamerri Group|42085|6|Mentioned|Fig.2 P374|||||||||
13823|Nappamerri Group|42395|5|Briefly described|Fig.13 P83|||In Qld, SA.||||||
13823|Nappamerri Group|42746|5|Briefly described|Fig.2 P4|||||||||
13823|Nappamerri Group|42999|5|Briefly described|Table 2,p90||Middle Triassic|||||||
13823|Nappamerri Group|43105|5|Briefly described|Fig.7,p13|||||||||
13823|Nappamerri Group|43570|6|Mentioned|Fig.2,p535|Scythian|Tatarian|||||||
13823|Nappamerri Group|43628|6|Mentioned|Fig.3|Late Triassic|Early Triassic|||||||
13823|Nappamerri Group|44133|4|Described|p78-79, 85|Middle Triassic|Late Permian|Geological Province: Cooper Basin. Overlies: Gidgealpa Group. Consists of: Arrabury Formation, Tinchoo Formation. Overlain by the Cuddapan Formation. Thickness:>550m.||||||17-JAN-08
13823|Nappamerri Group|60717|5|Briefly described|p40, p41|Middle Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Overlies the Gidgealpa Group. Max.  Thickness: 500m. Geological Province: Cooper Basin. See also Figure 2.||||||17-JUL-14
13823|Nappamerri Group|61015|6|Mentioned|p45|Triassic|Triassic|||||||19-APR-05
13823|Nappamerri Group|61613|6|Mentioned|p282, p282 Fig. 2|Triassic|Late Permian|Includes Arrabury and Tinchoo Formation. Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
13823|Nappamerri Group|61614|6|Mentioned|p294, p295, p290 Fig. 2|Middle Triassic|Late Permian|Includes Tinchoo and Arrabury Formations. Geological Province: Cooper Basin.||||||17-MAR-09
13823|Nappamerri Group|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304, p305|Late Triassic|Late Permian|Includes; Arrabury and Tinchoo Formations, Callamburra, Paning and Wimma Sandstone Members. Conformably overlies Toolachee Formation. Geological Province: Cooper Basin. Fluvial and lacustrine environments.||||||07-FEB-11
13823|Nappamerri Group|61616|6|Mentioned|p330 Fig. 2|Early Triassic|Late Permian|Includes Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||
13823|Nappamerri Group|62046|5|Briefly described|p125 Fig. 2|Triassic|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
13823|Nappamerri Group|62537|6|Mentioned|p191 Fig.2. |Late Triassic|Early Triassic|Cooper Basin.|||Includes Arrabury and Tinchoo Formations and Wimma Sandstone.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|62730|5|Briefly described|p351, p352 Fig. 1|Late Triassic|Late Permian|Includes the Arrabury and Tinchoo Formations. Geological Province: Cooper Basin.||||||21-APR-08
13823|Nappamerri Group|63832|6|Mentioned|p131 fig 2|Changhsingian|Changhsingian|Of Cooper Basin.||||||14-MAR-14
13823|Nappamerri Group|63978|2|Defined|p7, p18, Fig. 3|Early Triassic|Late Permian|Supersedes Nappamerri Fm. Contains the Arrabury and Tinchoo Fms. Max. thick: 450m. Conformable on Toolachee Fm (Gidgealpa Gp). Unconformably overlain by Poolawanna Fm and Hutton Sandstone (Eromanga Basin), and by Cuddapan Fm. in places. In Cooper Basin.||||||07-FEB-11
13823|Nappamerri Group|63979|6|Mentioned|p31|||||||||07-FEB-11
13823|Nappamerri Group|64048|5|Briefly described|p65|Triassic|Early Triassic|Includes the Tinchoo Formation. Member units act as a seal for the Toolachee Formation reservoirs.||||||07-FEB-11
13823|Nappamerri Group|64197|6|Mentioned|p625 Fig.1c|Middle Triassic|Late Permian|Cooper Basin.|||Includes the Arrabury and Tinchoo Formations|Overlies Toolachee Formation.||
13823|Nappamerri Group|64631|6|Mentioned|p44 Fig.2.||Changhsingian|Cooper Basin. Some biostratigraphic age control.||||Overlies Toolachee Formation.||
13823|Nappamerri Group|65489|5|Briefly described|p24-25, p42, p48, p96, p130-132, p158|Middle Triassic|Permian|Cooper Basin. Reservoir for economic oil and gas. The best source rocks are thin, laterally discontinuous coals in the upper part of the unit. Also regarded as a regional seal to the Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Overlies Gidgealpa Group unconformably (?) and Toolachee Formation conformably.||
13823|Nappamerri Group|65925|5|Briefly described|p16 Fig.2.3, Appendix 2.|Triassic|Triassic|Cooper Basin.|||||Red beds; mudstone; siltstone; sandstone; lithic sandstone.|
13823|Nappamerri Group|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Is unconformably overlain by Poolowanna Formation.||
13823|Nappamerri Group|67402|6|Mentioned|p90, p90 fig CPR4, p95|Middle Triassic|Late Permian|See also p96, p98, p100, p105.|||Includes the Arrabury Formation and Tinchoo Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p207|Middle Triassic|Lopingian|Nomenclatural history and subdivision of this group is outlined by Gray and McKellar (2002). Introduced by Papalia (1969, p.108). Raised to Group status by Powis (1989). Thickest in the Windorah and Arrabury troughs.|||Includes the Tinchoo Formation and Arrabury Formation (basal).|Unconformably overlain by the Poolawanna Formation and Hutton Sandstone or the Cuddapan Formation.|Contains distinct redbed characteristics.|17-JUL-14
13823|Nappamerri Group|69019|5|Briefly described|p82.|Middle Triassic|Permian|Southern Cooper Basin.|||||Dominated by fluvial sands.|
13823|Nappamerri Group|69023|5|Briefly described|p81-82, p151|Middle Triassic|Permian|Cooper Basin. Eroded by Middle Triassic tectonic activity causing tilting to the NE. Rocks of this unit are not known in the CALLABONNA sheet area.||||Conformably overlies Gidgealpa Group.||
13823|Nappamerri Group|69454|5|Briefly described|p38:4|Ladinian|Changhsingian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group.||12-JUL-16
13823|Nappamerri Group|69673|6|Mentioned|p153 fig 125||||||Includes Arrabury Formation, Tinchoo Formation|||
13823|Nappamerri Group|69728|6|Mentioned|p285|Late Triassic|Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||
13823|Nappamerri Group|69797|5|Briefly described|p17 Fig.2, p18|Middle Triassic|Early Triassic|Geol. Prov: Cooper Basin.|||Tinchoo Formation, Arrabury Formation|||
13823|Nappamerri Group|69946|5|Briefly described|p9, p52, p54|Late Triassic|Permian|Cooper Basin.|||Includes Arrabury and Tinchoo Formations.|Conformably overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69947|5|Briefly described|p13 Fig.7.2, p16-17 Figs.7.5-6|Middle Triassic|Late Carboniferous|See also p21 Fig.7.10. Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|69948|6|Mentioned|p3-4|Early Triassic|Permian|Cooper Basin. Basement to Eromanga Basin in the southern Cooper region.||||||
13823|Nappamerri Group|70317|6|Mentioned|p33|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|Overlies Gidgealpa Group. Is overlain unconformably by Cuddapan Formation.||
13823|Nappamerri Group|70823|4|Described|iv, p14, p25-p27|Middle Triassic|Lower Triassic|Cooper Basin. Seismic reflection and outcrop characteristics briefly discussed. This group has an average thickness of ~200m and is thickest in the Nappamerri Trough. This group is generally regarded as sealing the Gidgealpa Group. See also p39, p41, p49-p50, p70, p75-p77, p82.|||Includes the Arrabury Formation and the Tinchoo Formation.|Conformably overlies the Gidgealpa Group.||
13823|Nappamerri Group|70824|4|Described|p1, p5, p8, p37, p104-p107, p113, p123|Middle Triassic|Lower Triassic|Cooper Basin. Typically deposited as organically lean fluvial deposits. Areal extent and source rock geochemistry is discussed. This group reaches a maximum thickness close to 600m in the Nappamerri, Patchawarra and Arrabury troughs.|||Includes the Arrabury Formation and the Tinchoo Formation.|||
13823|Nappamerri Group|70946|5|Briefly described|p1087, p1089|Middle Triassic|Late Permian|Cooper Basin.|||Arrabury, Tinchoo Formations.|||08-OCT-18
13823|Nappamerri Group|71265|5|Briefly described|p589|Induan|Olenekian|Cooper Basin.|||Arrabury Formation.|Overlies Gidgealpa Group.||
13823|Nappamerri Group|71321|6|Mentioned|p15|||Of Patchawarra and Nappamerri troughs, Cooper Basin.||||||
13823|Nappamerri Group|71342|5|Briefly described|Ch4 p3-p4, Ch5 p9,  Ch5 p30|Early Triassic|Late Permian|Cooper Basin. See also Ch5 p52, Ch7 p13, Ch7 p16, Ch7 p21, Ch10 tbl 10.1, Ch10 p14, Ch10 p17, Ch10 p19-p20, Ch13 p7.|||Includes the Arrabury Formation and the Tinchoo Formation.|Overlies the Toolachee Formation. Unconformably overlain by the Hutton Sandstone.||
13823|Nappamerri Group|71701|5|Briefly described|p155|Olenekian|Induan|Cooper Basin.|||Includes the Arrabury Formation.|Overlies the Gidgealpa Group.||
13823|Nappamerri Group|72297|5|Briefly described|p742|||Cooper Basin. Has gas reservoirs at Marama and at Epsilon.||||||
13823|Nappamerri Group|72298|5|Briefly described|p801|Triassic||Eromanga Basin (SA,QLD).||||Is overlain unconformably by Poolowanna FZ.||
13823|Nappamerri Group|73167|5|Briefly described|p662, p664|Triassic|Triassic|Cooper Basin. Up to 500m of Nappamerri Group sediments uplifted and eroded along pre-existing faults in the Late Triassic E-W-compressional Hunter-Bowen Event, regional unconformity. Constituent units in Fig. 2, p664 confirmed in ASUD.|||Callamurra Member, Panning Member, Wimma Sandstone Member, Tinchoo Formation|Overlies the Toolachee Formation.|Floodplain, lacustrine and fluvial channel sediments.|
13823|Nappamerri Group|73244|6|Mentioned|p86|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels.||||||
13823|Nappamerri Group|73251|6|Mentioned|p62|Middle Triassic|Permian|Cooper Basin. Non-marine depositional environments.|||Tinchoo Formation, Arrabury Formation, Wimma Sandstone Member, Paning Member, Callamurra Member|Underlain by Toolachee Formation (Gidgealpa Group).||
13823|Nappamerri Group|73343|5|Briefly described|p337-338|Triassic|Triassic|Cooper Basin. Reflects floodplain, lacustrine, and fluvial channel settings. Incised during the Late Triassic Hunter-Bowen Event.|||Tinchoo Formation, Wimma Sandstone Member, Panning Member, Callamurra Member|Underlain by Toolachee Formation.||
13823|Nappamerri Group|73479|5|Briefly described|p156 Fig.2, p159, p163, p166|Triassic|Triassic|Cooper Basin. Floodplain, lacustrine, fluvial channels depositional environment. Highly efficient regional seal. Up to 500 m thickness was exhumed and eroded in Hunter-Bowen Event.|||Callamurra Member, Panning Member, Wiumma Sandstone Member, Tinchoo Formation|Overlies Toolachee Formation, unconformably underlies Cuddapan Formation||
13823|Nappamerri Group|73495|6|Mentioned|p498|Middle Triassic|Lower Triassic|Cooper Basin. Up to 550 m thick.||||||
13847|Naraku Granite|22460|6|Mentioned|Fig 1 p446.|||||||||
13847|Naraku Granite|22522|6|Mentioned|Fig2p332,Fig3p333|||||||||
13847|Naraku Granite|22667|6|Mentioned|p240||Calymmian|Age of unit is 1502+/-7 Ma (Page, 1993).||||||19-MAR-18
13847|Naraku Granite|22747|5|Briefly described|p8||Calymmian|1450 Ma. Intrudes Corella Formation only.||||||
13847|Naraku Granite|23068|5|Briefly described|p784 (Fig 1)|||||||||
13847|Naraku Granite|23070|5|Briefly described|p769 (fig 1)||Calymmian|||||||
13847|Naraku Granite|23071|5|Briefly described|p760|||||||||
13847|Naraku Granite|23458|5|Briefly described|p115 Fig.2, p129|||Parts referred to as ca 1500Ma suite and ca 1740Ma suite.||||||27-AUG-07
13847|Naraku Granite|23518|5|Briefly described|p12|||Geological Province: Western Fold Belt.||||||
13847|Naraku Granite|23519|5|Briefly described|p110 Table 1|||Geological Province: Eastern Fold Belt.||||||
13847|Naraku Granite|23959|5|Briefly described|p1166|Proterozoic|Proterozoic|Age: ~1754-1508Ma.  Geological Province: Mount Isa Inlier.||||||
13847|Naraku Granite|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
13847|Naraku Granite|23967|6|Mentioned|p1331 Fig.1|||||||||
13847|Naraku Granite|24168|6|Mentioned|p635|||||||||
13847|Naraku Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: ca1500Ma. Geological Province: Mount Isa Inlier. Name written as Naraku only under heading for GRANITE.||||||09-MAY-05
13847|Naraku Granite|30095|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13847|Naraku Granite|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13847|Naraku Granite|30531|6|Mentioned|p20|||Also mention p22.||||||19-MAR-18
13847|Naraku Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13847|Naraku Granite|31043|6|Mentioned|p57|||||||||
13847|Naraku Granite|32660|5|Briefly described|Table 5|||||||||
13847|Naraku Granite|32959|6|Mentioned|Fig.21|||||||||
13847|Naraku Granite|33791|6|Mentioned|p373|||||||||
13847|Naraku Granite|33900|6|Mentioned|p15|||||||||
13847|Naraku Granite|35074|6|Mentioned|Fig.2|||||||||
13847|Naraku Granite|35167|6|Mentioned|p154|||||||||
13847|Naraku Granite|35295|6|Mentioned|p602|||||||||
13847|Naraku Granite|35309|6|Mentioned|p373|||||||||
13847|Naraku Granite|35388|6|Mentioned|p89|||Also see Fig.10||||||
13847|Naraku Granite|36332|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic(Carpentarian)||||||
13847|Naraku Granite|37462|4|Described|Table4.VII|||||||||
13847|Naraku Granite|37568|6|Mentioned|p85|||||||||
13847|Naraku Granite|38278|6|Mentioned|Fig.3|||||||||29-SEP-04
13847|Naraku Granite|38833|6|Mentioned|p161|||||||||
13847|Naraku Granite|38900|6|Mentioned|p62|||||||||
13847|Naraku Granite|39445|6|Mentioned|p43|||See also Table 2||||||
13847|Naraku Granite|39798|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13847|Naraku Granite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
13847|Naraku Granite|40648|6|Mentioned|p11|||||||||
13847|Naraku Granite|40840|6|Mentioned|Map legend|||||||||
13847|Naraku Granite|41464|6|Mentioned|Map legend|Proterozoic||||||||
13847|Naraku Granite|41556|6|Mentioned|Map legend|Proterozoic||||||||
13847|Naraku Granite|41568|4|Described|p15|||||||||
13847|Naraku Granite|41791|6|Mentioned|Fig.1|||||||||
13847|Naraku Granite|41979|6|Mentioned|p527-528|||Age range is for Naraku batholith. See p527. The 1754 +/-25 Ma age is for a recrystallised microgranite near Cloncurry, a 1508+/-70 Ma age was determined for the southeastern coarse-grained pluton.||||||19-MAR-18
13847|Naraku Granite|42173|6|Mentioned|Fig.1 P172|||||||||
13847|Naraku Granite|42706|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Age: ~1500Ma.  Granite, generally non-foliated.||||||09-FEB-09
13847|Naraku Granite|43638|5|Briefly described|p59|||U-Pb age: 1754+/-25 Ma||||||
13847|Naraku Granite|44271|2|Defined|p37,46||Paleoproterozoic|||||||07-NOV-08
13847|Naraku Granite|44275|14|Not recorded|Map Legend|||||||||
13847|Naraku Granite|44278|4|Described|p5,map|||||||||
13847|Naraku Granite|44279|4|Described|p5,map|||||||||
13847|Naraku Granite|44849|14|Not recorded|p74|||||||||
13847|Naraku Granite|44989|2|Defined|p.148|||Tb.IV. On many pages. (E54-14,F54-2).||||||
13847|Naraku Granite|45003|14|Not recorded|p22,23|||||||||
13847|Naraku Granite|45166|5|Briefly described|p38|||||||||
13847|Naraku Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
13847|Naraku Granite|48906|14|Not recorded|p4,27|||||||||
13847|Naraku Granite|49041|5|Briefly described|Table 3|||||||||
13847|Naraku Granite|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
13847|Naraku Granite|50332|5|Briefly described|p22, p89|Mesoproterozoic|Mesoproterozoic|Of the Williams and Naraku Batholiths. Age: 1520-1450Ma. Geological Province: Quamby-Malbon and Cloncurry Subprovinces.||||||19-MAR-18
13847|Naraku Granite|60665|6|Mentioned|p1146|Calymmian|Calymmian|Postmetamorphic.|1550-1500 Ma.|Unit in Williams Suite.||||
13847|Naraku Granite|61830|6|Mentioned|p178|||||||||
13847|Naraku Granite|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
13847|Naraku Granite|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
13847|Naraku Granite|61936|5|Briefly described|p192 Fig. 5|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
13847|Naraku Granite|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks of the Williams Batholith - together with Williams Granite.||||||
13847|Naraku Granite|63593|5|Briefly described|p283, p285 Fig.1, p287, p288 Fig.2. |Mesoproterozoic|Mesoproterozoic|See also p289, p291, p293, p296-297. Also referred to in the article as Williams-Naraku granites (p283, 296, 298), Williams/Narabu [sic] Granite (in Fig.1), Williams and Naraku batholiths (p287), Williams and Naraku Granite (Fig.2), Williams-Naraku batholith (p289). Whichever name one picks, the authors suggest that fluids from these intrusions caused fluid over-pressuring, leading to extensive brecciation and related mineralization.|ca. 1500 Ma|||||
13847|Naraku Granite|64248|6|Mentioned|p33 Fig.1, p45|||||||||
13847|Naraku Granite|64250|6|Mentioned|p10 fig 2|||Immediately north of Cloncurry.||||||
13847|Naraku Granite|65396|6|Mentioned|p4 Fig.1, p22, p53 Fig.1, p104, p157|||See also p173, p213, p224, p272.||||||
13847|Naraku Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Mesoproterozoic|Mesoproterozoic|Williams Igneous Event.||Williams Supersuite|||Pink medium-grained biotite granite, aplite, pegmatite; locally albitised.|
13847|Naraku Granite|68542|6|Mentioned|p15|||Apparently associated with moderately high-temperature metamorphic magnetite veins at the old Ernest Henry quarry.||||||
13847|Naraku Granite|68576|6|Mentioned|Q_2: p15|||Apparently associated with moderately high-temperature metamorphic magnetite veins at the old Ernest Henry quarry.||||||
13847|Naraku Granite|69591|5|Briefly described|p59|||||Williams Supersuite.|||Pink, medium-grained biotite granite, aplite, pegmatite; locally albitised.|
13847|Naraku Granite|72297|6|Mentioned|p758|||NW of Quamby, NW QLD. Amethyst and quartz crystals occur in cockade-banded veins.||||||
13847|Naraku Granite|73553|6|Mentioned|p103, p206|||Williams-Naraku Igneous Province. Initially included Dipvale Granodiorite (Carter et al., 1961). Wilson et al., (1980) mapped subunits '1' (north) and '2' (south) of the Naraku Granite, subsequent mapping grouped these bodies as unnamed units PLg/l and PLg/l? (Withnall et al., 2016).||||||
13853|Narayen beds|23037|4|Described|p10,4,5,40,42,8,102,7,110,136|Late Permian|Early Permian|Possible correlation with the Buffel Formation.||||||
13853|Narayen beds|23042|4|Described|p8|||||||||
13853|Narayen beds|41246|6|Mentioned|Map legend|Permian||||||||
13853|Narayen beds|43008|5|Briefly described|map legend|||||||||
13853|Narayen beds|43017|5|Briefly described|Fig.3,p375|||||||||
13853|Narayen beds|50598|5|Briefly described|Map Legend|Early Permian|Early Permian|Dominantly andesitic conglomerate or breccia, sandstone and lava flows.||||||
13853|Narayen beds|60282|6|Mentioned|p4|||||||||
13853|Narayen beds|61777|5|Briefly described|p224, p228||Artinskian|Geological Province: Yarrol Province. May be correlatives of Camboon Volcanics. See p228 for more info. Rhyolitic to andesitic breccia and lava flows.||||||07-FEB-11
13853|Narayen beds|64398|5|Briefly described|Map legend|Early Permian|Early Permian|Dominantly andesitic (and lesser rhyolitic) conglomerate or breccia, sandstone, and lava flows; siltstone, lithic sandstone, subordinate conglomerate, and rare coquinite, limestone, and chert.||||||
13853|Narayen beds|64855|6|Mentioned|p29|Early Permian|Early Permian|||||||22-FEB-10
13853|Narayen beds|65388|3|Fully described|p43-46; p45, 13, 35, 36, 37, 114, 240|Early Permian|Early Permian|Whitaker and others (1974). Unconformably overlies Yerilla Metamorphics, Horse Granite Gneiss. May be part of Auburn Arch or Nogo Subprovince. Whitehouse (1936) suggested fossil plants  indicated Late Devonian or Carboniferous age. Intruded by Mount Saul Quartz Monzonite. Rhyolitic to dominantly andesitic rudite, arenite, and lava flows, lithic siltstone, sandstone, conglomerate and rare coquinite, limestone and chert. See also p312, 347, 432, 441, 447||||||
13853|Narayen beds|68008|5|Briefly described|p139|||Hutton et al. (1999).||||Unconformably overlies Dinner Creek Conglomerate. May be partial time equivalent of Owl Gully Volcanics.|Includes rhyolitic to dominantly andesitic breccia and lava flows.|
13853|Narayen beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Yarrol Province. Auburn Subprovince. This unit, with the Nogo and Smoky beds, and the Yaparaba Volcanics, are all mapped under the symbol, Pvy.||||||
13853|Narayen beds|68679|5|Briefly described|p312-313,p343-344,p351-354,p416,p418-419|Permian|Permian|Whitaker et al. (1974). Nogo Subprovince (Camboon Volcanic Arc), northern New England Orogen. Part of the Rawbelle Batholith. Crops out over ~300 km2, from Yerilla homestead to beyond Hawkwood homestead (and presumably further S under the Surat Basin).||||Is faulted against the Yerilla Metamorphics. Is intruded by Delubra, Jack Shay, Kenmore Gabbros, East Apple Granite. Correlated with Buffel Formation; probably correlated with Nogo beds.|Rhyolitic to dominantly andesitic flows, volcaniclastic sandstone, siltstone and conglomerate; rare coquinite locally with siliciclastic sandy layers alternating with layers of marine fossil fragments, limestone and chert.|
13927|Natal Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Quartzose and feldspathic sandstone, siltstone and mudstone.  Max. thickness: 1200m.  Geological Province: Drummond Basin.||||||
13927|Natal Formation|30151|6|Mentioned|p13|||Upper Devonian? - Lower Carboniferous. See also Fig.3.||||||
13927|Natal Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
13927|Natal Formation|31121|6|Mentioned|p384|||||||||
13927|Natal Formation|32138|6|Mentioned|Table 1|||||||||
13927|Natal Formation|32490|4|Described|Table 1|||L.Carb.||||||
13927|Natal Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13927|Natal Formation|32553|4|Described|p46|||||||||
13927|Natal Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13927|Natal Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13927|Natal Formation|34408|6|Mentioned|p185|||On table||||||
13927|Natal Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13927|Natal Formation|35811|6|Mentioned|Fig.3|||||||||
13927|Natal Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13927|Natal Formation|37573|4|Described|Table 2|||||||||
13927|Natal Formation|39445|5|Briefly described|Table 6|||||||||
13927|Natal Formation|41710|5|Briefly described|p225|||||||||
13927|Natal Formation|42486|5|Briefly described|p201|||||||||
13927|Natal Formation|42547|5|Briefly described|Fig.17 P61|||||||||
13927|Natal Formation|43105|6|Mentioned|p12|||||||||
13927|Natal Formation|45073|3|Fully described|p44|||Refers Olgers (1969b)||||||
13927|Natal Formation|45151|5|Briefly described|Table 6|||||||||
13927|Natal Formation|46881|6|Mentioned|Table 2|||||||||
13927|Natal Formation|48914|6|Mentioned|p35|||L.Carb.||||||
13927|Natal Formation|60659|5|Briefly described|p14, p91|||Montonous sequence of thin, well-bedded, fine-grained feldspathic quartz sandstone with interbedded olive-green siltstone and mudstone. Conformably overlies Bulliwallah Formation. Geological Province: Drummond Basin.||||||07-FEB-11
13927|Natal Formation|64849|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Alternating fine feldspathic quartz sandstone and olive siltstone; poorly preserved plant fossils.||||||
13927|Natal Formation|64850|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Alternating fine feldspathic quartz sandstone and olive siltstone; poorly preserved plant fossils.||||||
13927|Natal Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Alternating fine feldspathic quartz sandstone and olive siltstone; poorly preserved plant fossils.||||||10-FEB-09
13927|Natal Formation|66188|6|Mentioned|435, 437, 441, Fig 3, TB1, Fig 16-17|Early Carboniferous|Early Carboniferous|Northern Galilee Basin. Dated using fish specimens and is equivalent to the Ducabrook Formation in the Drummond Basin.||||||
13927|Natal Formation|67402|4|Described|p165 tbl LPB1, p196 fig DRM2|Visean|Visean|Drummond Basin. Deposited in a lacustrine or braided/delta environment. Siltstones and mudstones are the best potential seal untis in the Drummond Basin. Approximately 400m thick. See also p197, p198 fig DRM3, p200, p201, p202, p203 fig DRM11, p308.||||Overlies the Bulliwallah Formation.|Interbedded fine-grained feldspathic quartz sandstone, olive green siltstone and mudstone.|
13927|Natal Formation|68329|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Conformably overlies Bulliwallah Formation.|Alternating fine feldspathic quartz sandstone and olive siltstone; poorly preserved plant fossils.|
13927|Natal Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Bulliwallah, Ducabrook, Mount Rankin and Star of Hope Formations, are all mapped under the symbol, Cd3.||||||
13927|Natal Formation|68731|5|Briefly described|p191 Fig 3.102, p195, p203|Mississippian|Mississippian|Drummond Basin. Local siliceous nodules contain fish and plant remains (Turner and Cook 1999).||||Underlain by the Bulliwallah Formation.|Comprises thin, fine, quartzofeldspathic sandstone with common cross-lamination and ripple marks. Contains subordinate interbeds of siltstone and mudstone that are variably calcareous and carbonaceous.|17-JUL-14
13927|Natal Formation|68900|2|Defined|p4, p37, p70, p72|Carboniferous|Carboniferous|Drummond Basin. Originally named by Olgers (1969) after Natal Downs homestead in northern NATAL DOWNS. Olgers (1972) specified a reference section along the track to Peggurrimma yard north-east of Natal Downs homestead. This unit is distinguished from the Bulliwallah Formation by its uniform thin-beddin, fine-grain size and good sorting. This unit in general produces low topography but in some locations produces hilly topography such as Mount Helena. In geophysics the unit produces a bright pink signature indicating high potassium whilst it is also non magnetic. Interpreted to have been deposited in a low-energy, fluvio-lacustrine environment. Up to 1200m of Natal Formation crops out north-east of Natal Downs, however the lack of preservation of the top of the formation means the original thickness is not known. Poorly preserved plant fossils suggest a Carboniferous age. Probably a time equivalent of the Ducabrook Formation.||||Conformably overlies the Bulliwallah Formation.|Moderately to poorly-sorted, very fine- to fine-grained, thin- to medium-bedded and flaggy sandstone, light brown, very thin- to thin-bedded siltstone. Rare coarse grained sandstones also occur.|
13927|Natal Formation|71710|5|Briefly described|p370, p374 Fig 8, p375, p384, p385|Early Carboniferous|Early Carboniferous|Geological province: northern Drummond Basin.||||Unconformably overlain by Lake Galilee Sandstone. Underlain by Bulliwallah Formation. Equivalent to upper part of Ducabrook Formation.||22-MAY-19
13927|Natal Formation|73198|4|Described|p499-501, p505-511, p514-515|||Drummond Basin, north. Originally part of Cycle 3 of Olgers (1972); combined with Cycle 2 herein. Maximum thickness: 1200 m. Minimum thickness of 202 m. Relatively consistent thickness. Observed in this study to mark a pronounced and abrupt change to persistent coarse-grained, erosionally based facies, with few siltstones and no volcanic or volcaniclastic beds. Coarse grain size reported here contrasts with fine grain size reported previously (i.e., Olgers, 1972). A gradual fining-upward trend is apparent throughout the succession. Compositionally indistinguishable from [previous] Cycle 2. Mixed basement / volcanic provenance. [See article for petrographic descriptions and data].||||Conformably underlain by Bulliwallah Formation. Equivalent to Ducabrook Formation.|[Well] sorted, uniformly thin bedded, quartz to feldspathic sandstone with minor siltstone and mudstone, and no volcanic or volcaniclastic beds.|
13930|Native Bee Siltstone|22453|5|Briefly described|p 11  Fig 10|||||||||
13930|Native Bee Siltstone|22665|6|Mentioned|P221, Table1|||||||||
13930|Native Bee Siltstone|22836|6|Mentioned|Fig.10 p402|||||||||
13930|Native Bee Siltstone|23031|5|Briefly described|27|||Geol province Leichardt River Subprovince. Parent Mount Isa Group. Underlying unit Breakaway Shale||||||
13930|Native Bee Siltstone|23397|5|Briefly described|p467 Fig.2|||||||||
13930|Native Bee Siltstone|23398|5|Briefly described|p454|||Of Mount Isa Group.||||||
13930|Native Bee Siltstone|23399|4|Described|p495|Statherian|Statherian|of Mount Isa Group,||||||
13930|Native Bee Siltstone|23408|5|Briefly described|p511, p512, p513 Fig. 2|||Prominent marker horizon in the Mount Isa Group. Contains stromatolites, halite pseudomorphs, flat pebble conglomerates and x-beddec chammel deposits.||||||15-JUN-09
13930|Native Bee Siltstone|23466|5|Briefly described|p269|||||||||
13930|Native Bee Siltstone|23518|4|Described|p12|Proterozoic|Proterozoic|Of Mount Isa Group.  Geological Province: Western Fold Belt.||||||
13930|Native Bee Siltstone|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: Mount Isa Group||||||07-NOV-08
13930|Native Bee Siltstone|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Laminated chert (lower unnamed member), and overlying thinly bedded dolomite, sandy dolomite and coarse siltstone. Conformably overlies Breakaway Shale.  Part of the Gun Supersequence.||||||07-NOV-08
13930|Native Bee Siltstone|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group.  Overlies the Breakaway Shale; underlies the Urquhart Shale.||||||25-AUG-04
13930|Native Bee Siltstone|30535|6|Mentioned|p405|||Refers type section. See also P403. Refers Bennett(1965)||||||
13930|Native Bee Siltstone|31207|6|Mentioned|p1415|||||||||
13930|Native Bee Siltstone|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13930|Native Bee Siltstone|32041|4|Described|p355|||||||||
13930|Native Bee Siltstone|32042|4|Described|p39|||||||||
13930|Native Bee Siltstone|32376|6|Mentioned|Table 3|||||||||
13930|Native Bee Siltstone|32660|5|Briefly described|Table 5|||||||||
13930|Native Bee Siltstone|32959|6|Mentioned|Fig.21|||||||||
13930|Native Bee Siltstone|33900|5|Briefly described|p14|||||||||
13930|Native Bee Siltstone|34499|6|Mentioned|Table 1|||||||||
13930|Native Bee Siltstone|34754|6|Mentioned|p42|||||||||
13930|Native Bee Siltstone|35074|6|Mentioned|Fig.2|||||||||
13930|Native Bee Siltstone|35116|6|Mentioned|Table.4|||||||||
13930|Native Bee Siltstone|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13930|Native Bee Siltstone|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13930|Native Bee Siltstone|37568|5|Briefly described|p84|||||||||
13930|Native Bee Siltstone|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13930|Native Bee Siltstone|38348|6|Mentioned|p11|||||||||
13930|Native Bee Siltstone|38350|4|Described|p15|||||||||
13930|Native Bee Siltstone|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13930|Native Bee Siltstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
13930|Native Bee Siltstone|39445|5|Briefly described|Table 2|||||||||
13930|Native Bee Siltstone|39492|6|Mentioned|p31|||||||||
13930|Native Bee Siltstone|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
13930|Native Bee Siltstone|39561|6|Mentioned|Fig.8|||||||||
13930|Native Bee Siltstone|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of Mount Isa Group. Dolomitic siltstone, dolomite.||||||15-JUN-06
13930|Native Bee Siltstone|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
13930|Native Bee Siltstone|39934|6|Mentioned|p318|||||||||
13930|Native Bee Siltstone|40623|5|Briefly described|p101|||||||||
13930|Native Bee Siltstone|41248|6|Mentioned|Fig.2|||||||||
13930|Native Bee Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
13930|Native Bee Siltstone|41307|4|Described|p16|||||||||
13930|Native Bee Siltstone|42350|6|Mentioned|Fig.1 P543|||||||||
13930|Native Bee Siltstone|42782|6|Mentioned|p458|||of Mount Isa Group||||||
13930|Native Bee Siltstone|44517|2|Defined|p235,map||Paleoproterozoic|Unit of Mount Isa Group. Replaces "Golf Course Siltstone".||||||07-NOV-08
13930|Native Bee Siltstone|45072|4|Described|Table 9|||Chem. anal. See also pp37-38.||||||15-JUN-09
13930|Native Bee Siltstone|45136|5|Briefly described|p50|||||||||
13930|Native Bee Siltstone|45161|5|Briefly described|Table 8|||||||||
13930|Native Bee Siltstone|45166|5|Briefly described|p28|||||||||
13930|Native Bee Siltstone|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
13930|Native Bee Siltstone|47083|5|Briefly described|p19|||Equivalent to Paradise Creek Formation. Of Mount Isa Group.||||||
13930|Native Bee Siltstone|50332|5|Briefly described|p21, p95|Proterozoic|Proterozoic|Of the Mount Isa Group. Conformably underlain by Breakaway Shale. Geol Prov: Western Fold Belt Province.||||||07-FEB-11
13930|Native Bee Siltstone|50550|6|Mentioned|p1141 Fig.4||Statherian|Of Mount Isa Group. Geological Province: Western Fold Belt.||||||19-DEC-07
13930|Native Bee Siltstone|50624|5|Briefly described|p237 Fig.4||Statherian|Parent: Mount Isa Group. Overlain by Urquhart Shale.||||||24-NOV-04
13930|Native Bee Siltstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Isa Group. Dolomitic siltstone, shale.||||||
13930|Native Bee Siltstone|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Overlain by Urquhart Shale, underlain by Breakaway Shale. Geological Province: Western Fold Belt.||||||
13930|Native Bee Siltstone|61736|5|Briefly described|p674|||Of the Mount Isa Group. Fine Silty dolomite.||||||
13930|Native Bee Siltstone|61923|5|Briefly described|p29 Fig.2|||Of the Mount Isa Group. Characterised by multicoloured siltstone and interlayered fine sandstone, increasingly dolomitic and ferruginous upsection. Overlies Breakaway Shale; overlain by Urquhart Shale. Geol Prov: Mount Isa Inlier.||||||
13930|Native Bee Siltstone|62084|5|Briefly described|p936 Fig.5, p951 Fig.15|||Isa Superbasin. Mount Isa. Shown as Native Bee Slst in Fig.5.||Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
13930|Native Bee Siltstone|62535|5|Briefly described|p672, p674|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.||Mount Isa Group.|||Includes fine, silty dolomite.|
13930|Native Bee Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
13930|Native Bee Siltstone|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
13930|Native Bee Siltstone|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Gun supersequence.||||||
13930|Native Bee Siltstone|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Native Bee.||||||
13930|Native Bee Siltstone|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
13930|Native Bee Siltstone|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
13930|Native Bee Siltstone|63866|5|Briefly described|p59|Statherian|Statherian|Isa Superbasin.|1655 +/- 4 Ma (Page et al., 2000)|Gun Supersequence||||
13930|Native Bee Siltstone|64250|5|Briefly described|p11 fig 3, p24 |||||Unit in Mount Isa Group.|||Contains rhythmically laminated turbidite in upper part.|
13930|Native Bee Siltstone|65396|5|Briefly described|p82, p175, p197, p241|||Isa Superbasin. Cover Sequence 3. Leichhardt River Fault Trough.||Mount Isa Group||Overlies Breakaway Shale; overlain by Urquhart Shale.|Rhythmically-laminated turbidite deposits.|
13930|Native Bee Siltstone|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
13930|Native Bee Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p26, p34. Leichhardt River Domain, Mount Isa Inlier. Isa Superbasin.|~1660-1650 Ma.|Of Mount Isa Group.|||Dolomitic siltstone, dolomite, siliceous siltstone, chert.|
13930|Native Bee Siltstone|68542|6|Mentioned|p6|||||||Overlies Breakaway Shale, overlain by Urquhart Shale||
13930|Native Bee Siltstone|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Breakaway Shale. Is overlain by Urquhart Shale.||
13930|Native Bee Siltstone|68732|6|Mentioned|p160, p162, p163, p168|||||Mount Isa Group.||||01-DEC-17
13930|Native Bee Siltstone|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||Mount Isa Group||||
13930|Native Bee Siltstone|69591|5|Briefly described|p43 Fig.2.31, p45|||Isa Superbasin. Part of Gun Supersequence. Deposited below storm base.||Mount Isa Group.|||Dolomitic siltstone, dolomite, siliceous siltstone, chert.|
13930|Native Bee Siltstone|70282|6|Mentioned|p544 Fig.1|||Cover sequence 2, Mount Isa.||||Overlain by Urquhart Shale||13-FEB-18
13930|Native Bee Siltstone|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Dolomitic siltstone, dolomite, siliceous siltstone and chert; laminated chert marker beds at base. (Separately mapped) algal chert.|
13930|Native Bee Siltstone|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||Dolomitic siltstone, dolomite, siliceous siltstone and chert; laminated chert marker beds at base. (Separately mapped) algal chert.|
13930|Native Bee Siltstone|71960|4|Described|p85, p87, p77, p82|Proterozoic|Proterozoic|Base of second 'fining upward megasequence'  - upper Mount Isa Group. Top not preserved in Hero/Western Fault Zone, so 510m is minimum thickness. Three unnamed members discussed. Channel fill sands within a floodplain to carbonate mudflat. Overlying formations are lake deposits, saline mudflats and fan fringe deposits.||Of Mount Isa Group.|||Upper and lower: easily eroded thin bedded ferruginous shaly siltstone with sandy beds. Middle: massive shale, black siltstone; some stromatolitic chert beds. Includes coarser clastic sandstone bodies than underlying 'lower Mount Isa Group' units.|
13930|Native Bee Siltstone|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|Paroo Range, Hero/Western Fault Zone.||Of Mount Isa Group|||Shale, siltstone, sandstone lenses; massive shale, balck siltstone, chert; ferruginous shale, siltstone, some sandstone|
13930|Native Bee Siltstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Overlies Breakaway Shale and underlies Urquhart Shale.||
13930|Native Bee Siltstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||Mount Isa Group||Overlies Breakaway Shale and underlies Urquhart Shale.||
13930|Native Bee Siltstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Isa Superbasin.||Mt Isa Group||Underlain by Breakaway Shale. Overlain by Urquhart Shale.||
13930|Native Bee Siltstone|73525|6|Mentioned|p4-5 Fig.2|||Leichhardt River Domain.|||||Carbonates.|
13932|Native Cat Andesite|24491|4|Described|p23|Triassic|Triassic|||||||
13932|Native Cat Andesite|24571|6|Mentioned|p13, 19|||See also p22||||||
13932|Native Cat Andesite|24615|5|Briefly described|CD|Triassic|Triassic|[Rvn].  Andesite, andesitic tuff, trachyandesite, andesitic to rhyolitic breccia, minor rhyolite.||||||
13932|Native Cat Andesite|30451|6|Mentioned|p69|||||||||
13932|Native Cat Andesite|30811|6|Mentioned|p532|||||||||
13932|Native Cat Andesite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
13932|Native Cat Andesite|31657|4|Described|p96|||Triassic||||||
13932|Native Cat Andesite|31658|6|Mentioned|Map legend|Triassic|Triassic|||||||
13932|Native Cat Andesite|31659|2|Defined|p72|Triassic|Triassic|Max. thickness: ~1000ft. Andesitic lavas, tuff and lapilli tuff, minor trachyandesite. See also Table 1.||||||08-OCT-08
13932|Native Cat Andesite|32358|4|Described|Table 3|||P16||||||
13932|Native Cat Andesite|34408|6|Mentioned|p185|||On Table||||||
13932|Native Cat Andesite|35007|6|Mentioned|p77|||||||||
13932|Native Cat Andesite|35069|6|Mentioned|Fig.1|||||||||
13932|Native Cat Andesite|36576|6|Mentioned|p606|||||||||
13932|Native Cat Andesite|37565|6|Mentioned|p8|||||||||
13932|Native Cat Andesite|37611|6|Mentioned|p269|||See also Fig.2||||||
13932|Native Cat Andesite|37860|6|Mentioned|Fig.2|||||||||
13932|Native Cat Andesite|38081|5|Briefly described|Table 1|||||||||
13932|Native Cat Andesite|38406|6|Mentioned|p12|||||||||
13932|Native Cat Andesite|39445|5|Briefly described|Table 9|||||||||
13932|Native Cat Andesite|41246|6|Mentioned|Map legend|Triassic||||||||
13932|Native Cat Andesite|41576|4|Described|p19|||See also Table 1||||||
13932|Native Cat Andesite|41577|6|Mentioned|Map legend|Triassic||||||||
13932|Native Cat Andesite|41922|4|Described|Table 1, P9|||||||||
13932|Native Cat Andesite|50209|5|Briefly described|Map Legend|Triassic|Triassic|||||||
13932|Native Cat Andesite|50317|5|Briefly described|Map Legend|Triassic|Triassic|Andesite, andesitic tuff, trachyandesite, andesitic to rhyolitic breccia, minor rhyolite.||||||09-JUN-04
13932|Native Cat Andesite|60557|5|Briefly described|p19 Fig. 5b, p27|Triassic|Triassic|Andesitic volcanic succession.  Unconformably overlies the Dinner Creek Conglomerate.||||||09-JUN-05
13932|Native Cat Andesite|61782|5|Briefly described|p282|Middle Triassic|Middle Triassic|Overlies the Moah Creek Beds/Dinner Creek Conglomerate.||||||
13932|Native Cat Andesite|65388|6|Mentioned|p208|||Monto - Calliope area. Correlated with Muncon Volcanics.||||||
13932|Native Cat Andesite|65452|5|Briefly described|p2-4, p35-36|Late Triassic|Middle Triassic|Southern Yarrol Province. Age based on stratigraphic relationships and correlation with other units. Similar geochemistry to Agnes Water Volcanics. Trace elements briefly described.|||||Dominantly andesitic flows, tuff, andesitic to rhyolitic breccia. Minor rhyolitic flows towards top of sequence.|
13932|Native Cat Andesite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
13932|Native Cat Andesite|68008|3|Fully described|p70, p143, p153, p182-183, p188-191|Triassic|Triassic|See also p195-196, p209, p233, p244, p246, p251, p253-254, p259, p261, p264, p483, p485, p530. Kirkegaard et al (1970). Named after Native Cat Range, their type area. These rocks had been considered equivalent to the "Lower Bowen Volcanics" by Reid and Morton (1928). Caps a dissected plateau. Geochemistry detailed; one sample is almost identical with Bobby Volcanics. c.300m thick. Radiometric dating attempts have failed due to pervasive alteration; Rb-Sr data tabulated. Has simiar geochemistry and geological setting to Muncon Volcanics. Hosted rich alluvial and eluvial gold deposits sourced from an intrusion at Kalapa North. Is faulted against and underlies Stanwell Formation.||||Unconformably overlies Dinner Creek Conglomerate. Is overlain unconformably by Mount Salmon Volcanics, Alton Downs and Dalma Basalts, and ?Precipice Sandstone.|Mainly andesitic flows, andesitic tuff, lapilli tuff, trachyandesite, andesitic to rhyolitic breccias, and minor rhyolite flows.|
13932|Native Cat Andesite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Toogoolawah Group and Muncon Volcanics, are all mapped under the symbol, Rvm.||||||
13932|Native Cat Andesite|68679|5|Briefly described|p312-313, p338, p434, p444, p471|Late Triassic|Late Triassic|Crops out near Stanwell, northern New England Orogen. Forms a high, steeply dissected plateau (the Native Cat Range). ~300m thick. Magmatic arc during the Hunter-Bowen Orogeny. Age unknown.||||Correlated with Muncon Volcanics.|A flat-lying succession of porphyritic andesitic lavas and tuffs, andesitic to rhyolitic breccias and minor rhyolitic lavas.|
13932|Native Cat Andesite|73450|6|Mentioned|p52|Triassic|Triassic|||||Unconformably overlain by Mount Salmon Volcanics.||
13946|Neara Volcanics|13516|5|Briefly described|p159 fig 8|Triassic|Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
13946|Neara Volcanics|22757|5|Briefly described|p14||Triassic|Overlain by Ipswich Coal Measures.||||||18-AUG-08
13946|Neara Volcanics|22845|6|Mentioned|p11,18,21,46,57,82||Triassic|||||||
13946|Neara Volcanics|22846|6|Mentioned|p9,14,36,56,67|Middle Triassic|Early Triassic|Overlie  Gallangowan Granodiorite.||||||
13946|Neara Volcanics|23440|4|Described|p140|Triassic|Triassic|Of Toogoolawah Group.||||||18-AUG-08
13946|Neara Volcanics|23608|5|Briefly described|p50 Fig 1, p53|Carboniferous|Devonian|Intruded by Woolooga Granodiorite.||||||
13946|Neara Volcanics|23799|3|Fully described|p40, p37 Tb. 3, p37 Tb. 3|Middle Triassic|Early Triassic|Formerly "Lower Esk Series" of Hill (91930) and "Neara Series" of Bryan & Jones (1946).  Overlie Marumba beds, Claddagh Granodiorite and Mount Clara beds in east Esk Trough. Intruded by Kingaham Creek Granodiorite.Geological Province: Esk Trough.||||||12-NOV-15
13946|Neara Volcanics|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||
13946|Neara Volcanics|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 1000m.||||||
13946|Neara Volcanics|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Volcaniclastic conglomerate, andesite, sandstone.||||||
13946|Neara Volcanics|29420|6|Mentioned|p98|||||||||
13946|Neara Volcanics|29720|6|Mentioned|Fig.1|||||||||
13946|Neara Volcanics|29968|6|Mentioned|p11|||||||||
13946|Neara Volcanics|30089|6|Mentioned|p853|||||||||
13946|Neara Volcanics|30302|6|Mentioned|p414|||Lower to Middle Triassic age||||||
13946|Neara Volcanics|30451|6|Mentioned|p69|||||||||
13946|Neara Volcanics|30466|6|Mentioned|p1|||Triassic age||||||
13946|Neara Volcanics|30473|6|Mentioned|p377|||Refers Cranfield & Schwarzbock(1972). Part of Toogoolawah Group.||||||
13946|Neara Volcanics|31450|6|Mentioned|p46|||||||||
13946|Neara Volcanics|31451|6|Mentioned|p78|||||||||
13946|Neara Volcanics|31811|6|Mentioned|Fig. 1|||||||||
13946|Neara Volcanics|33381|4|Described|p109|||Triassic. See also PP113,117,122.||||||
13946|Neara Volcanics|34010|6|Mentioned|Cor. chart|||M.Triassic||||||
13946|Neara Volcanics|34261|6|Mentioned|p100|||P99 refers Zimmerman (1956)||||||
13946|Neara Volcanics|34974|6|Mentioned|p946|||||||||
13946|Neara Volcanics|35101|3|Fully described|p38|||||||||
13946|Neara Volcanics|35161|6|Mentioned|p591|||||||||
13946|Neara Volcanics|35427|6|Mentioned|p122|||||||||
13946|Neara Volcanics|36246|6|Mentioned|p15|||||||||
13946|Neara Volcanics|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
13946|Neara Volcanics|36926|6|Mentioned|p175|||||||||
13946|Neara Volcanics|36954|6|Mentioned|p114|||See Fig.1.||||||
13946|Neara Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
13946|Neara Volcanics|37376|6|Mentioned|p491|||||||||
13946|Neara Volcanics|37755|6|Mentioned|p79|||||||||
13946|Neara Volcanics|38304|6|Mentioned|p83|||||||||
13946|Neara Volcanics|39079|5|Briefly described|p8|||||||||
13946|Neara Volcanics|39445|5|Briefly described|Table 9|||See also Fig.7||||||
13946|Neara Volcanics|39505|6|Mentioned|p191|||||||||
13946|Neara Volcanics|40051|4|Described|p8|||||||||
13946|Neara Volcanics|40245|6|Mentioned|p182|||Mention P187||||||
13946|Neara Volcanics|40475|5|Briefly described|p8|||||||||
13946|Neara Volcanics|40477|6|Mentioned|p16|||||||||
13946|Neara Volcanics|40478|5|Briefly described|p24|||||||||
13946|Neara Volcanics|40479|6|Mentioned|p33|||||||||
13946|Neara Volcanics|40480|6|Mentioned|p39|||||||||
13946|Neara Volcanics|40484|6|Mentioned|Fig.2|||||||||
13946|Neara Volcanics|40623|5|Briefly described|p65|||||||||
13946|Neara Volcanics|41161|6|Mentioned|Fig.1|||||||||
13946|Neara Volcanics|41272|5|Briefly described|M 1of1 G15|||||||||
13946|Neara Volcanics|41591|5|Briefly described|p17|||||||||
13946|Neara Volcanics|41738|6|Mentioned|p163|||||||||
13946|Neara Volcanics|41917|6|Mentioned|p522|||||||||
13946|Neara Volcanics|42041|6|Mentioned|p222|||||||||
13946|Neara Volcanics|42492|5|Briefly described|Table 2 P14|||||||||
13946|Neara Volcanics|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
13946|Neara Volcanics|42619|5|Briefly described|p29|||||||||
13946|Neara Volcanics|42694|5|Briefly described|map legend|Triassic||||||||
13946|Neara Volcanics|42902|5|Briefly described|p416|||||||||
13946|Neara Volcanics|43003|6|Mentioned|Fig.16,p168|||||||||
13946|Neara Volcanics|43092|4|Described|p29|Middle Triassic|Early Triassic|see also map enclosure.||||||
13946|Neara Volcanics|43993|14|Not recorded|p102|||Ref. to Bryan and Jones 1946.||||||
13946|Neara Volcanics|44026|14|Not recorded|p122-125||Triassic|Conformably overlies Bryden Beds. Lithologically equivalent to Blackwall Breccia, Weir Basalt, Mount Crosby Formation.||||||
13946|Neara Volcanics|44076|14|Not recorded|Fig.38,p269,271-4|||||||||
13946|Neara Volcanics|44091|14|Not recorded|p52||Triassic|||||||
13946|Neara Volcanics|44360|14|Not recorded|p20||Triassic|Equivalent to Muncon Volcanics.||||||
13946|Neara Volcanics|44573|14|Not recorded|p95|||||||||
13946|Neara Volcanics|44671|2|Defined|p249||Early Triassic|See also Lexicon.||||||
13946|Neara Volcanics|44781|14|Not recorded|p365|||||||||
13946|Neara Volcanics|44783|14|Not recorded|p2,33-35|||||||||
13946|Neara Volcanics|44786|14|Not recorded|p193-202||Middle Triassic|||||||
13946|Neara Volcanics|44814|14|Not recorded|p483,485||Late Triassic|||||||
13946|Neara Volcanics|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
13946|Neara Volcanics|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group||||||30-NOV-05
13946|Neara Volcanics|45110|6|Mentioned|p80|||||||||
13946|Neara Volcanics|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group. Geological Province: Esk Trough (Wandilla Province).||||||18-AUG-08
13946|Neara Volcanics|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Volcanic conglomerate, agglomerate, andesitic tuff, lahar, shale, sandstone.||||||19-JUL-04
13946|Neara Volcanics|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Volcaniclastic conglomerate; andesite, sandstone; mudstone, siltstone laminae; conglomerate.||||||
13946|Neara Volcanics|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group. Geological Province: Esk Trough. Volcaniclastic conglomerate; andesite, sandstone.||||||12-NOV-15
13946|Neara Volcanics|60993|6|Mentioned|p8 Tb. 2|||Geological Province: Clarence-Moreton Basin.||||||
13946|Neara Volcanics|61003|6|Mentioned|p224|Middle Triassic|Middle Triassic|||||||
13946|Neara Volcanics|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Esk Trough.||||||17-MAR-09
13946|Neara Volcanics|61782|5|Briefly described|p275, p277, p277 Fig. 3, p282|||Geol Prov: Esk Trough. Volcaniclastic sedimentary rocks and minor intermediate voolcanics.||||||
13946|Neara Volcanics|63821|6|Mentioned|p20|||||||||07-FEB-11
13946|Neara Volcanics|65668|6|Mentioned|p20|Middle Triassic|Middle Triassic|Age: 240.9 Ma. Intruded by Elgin Vale Diorite.||||||10-JAN-17
13946|Neara Volcanics|67203|5|Briefly described|p3, p36-37|Late Triassic|Late Triassic|Further geochronological work is required to test the correlation with Mount Marcella Volcanics, and determine the southern extent of Late Triassic volcanism.||||Equivalent to Mount Marcella Volcanics.||12-NOV-15
13946|Neara Volcanics|67402|5|Briefly described|p204, p205 tbl ESK/ABR1|Ladinian|Ladinian|Esk Trough. Deposited in a fluvial environment. Approximately 500m thick. Contains a potential intraformational shale seal. See also p206 fig ESK/ABR6, p208-p210.||Toogoolawah Group||Overlies the Bryden Formation. Overlain by the Ipswich Coal Measures.|Agglomerate, conglomerate, andesitic flows, tuffs and fossiliferous shales.|
13946|Neara Volcanics|67874|5|Briefly described|p11, p19, p35|Middle Triassic|Early Triassic|Cranfield (1989). Age is based largely on poorly-constrained plant fossils and limited radiometric age data.|~240 Ma.|||Equivalent to Mount Marcella Volcanics.||
13946|Neara Volcanics|68679|4|Described|p322, p326, p328-329, p331-332, p387|Middle Triassic|Early Triassic|See also p389-391, p411, p427, p429, p433, p440, p471. Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Widespread unit. Nine subdivisions are tabulated and described in some detail, reflecting spatial variations more than stratigraphic units. Differing stratigraphic interpretations discussed. Rich in plant fossils (species listed). RELATED UNITS (continued): Is faulted against the Rocksberg Greenstone and Wongella Metamorphics. Is intruded by Elgin Vale Diorite, Avoca Creek and Boonara Granodiorites, and Somerset Dam Igneous Complex.|241.2 +/- 11 Ma; 239.2 +/- 5 Ma (Campbell, 2005).|Toogoolawah Group.||Unconformably overlies Amamoor, Maronghi Creek beds, Kandanga Creek Megabreccia, Kingaham Creek Granodiorite and Mount Mia Serpentinite. Underlies concordantly Aranbanga Volcanic Group. See COMMENTS.|Volcaniclastic conglomerate, andesitic volcanics, sandstone, andesite boulder beds, mudstone, conglomerate, dacitic volcanics, hornfels, felsic volcanics, volcaniclastic sandstone. All elaborated in detail on p390.|
13946|Neara Volcanics|69952|6|Mentioned|p4, p47, p49|Early Triassic|Early Triassic|||||||
13946|Neara Volcanics|72297|5|Briefly described|p712|||Kilkivan area.|||||Contains multiphase carbonate quartz veins hosting cinnabar veinlets and disseminations in NNW-trending fracture zones.|
13946|Neara Volcanics|73306|5|Briefly described|p565-566|Middle Triassic|Middle Triassic|Esk Trough.|c.242 Ma (Campbell, 2005).|Toogoolawah Group.|||Intermediate volcanic rocks.|
13946|Neara Volcanics|73450|6|Mentioned|p107|||||||||
13974|Neilson Leucogabbro|23042|5|Briefly described|p105|||||||||
13974|Neilson Leucogabbro|40577|3|Fully described|p54|||||||||
13974|Neilson Leucogabbro|40954|6|Mentioned|p133|||||||||
13974|Neilson Leucogabbro|61917|5|Briefly described|Map legend|Tertiary|Tertiary|Dark grey to black, coarse-grained biotite-augite-olivine leucogabbro to quartz gabbro.||||||
13974|Neilson Leucogabbro|65388|4|Described|p420, 421 ,422, p403 Fig. 135|Oligocene|Eocene|Oldest phase of Mount Jukes Intrusive Complex. Surrounds Jukes Granite. Equigranular, coarse-grained quartz gabbro.||||||
13974|Neilson Leucogabbro|69599|5|Briefly described|p634|||3km across. Forms a broad annular valley around Mount Jukes.||Mount Jukes Intrusive Complex.||Is intruded by Jukes Granite.|Gabbro; minor phases of syenite form ring dykes and other dykes intruding the outer margin and the aureole.|
13974|Neilson Leucogabbro|73450|4|Described|p45, p72-73|||Recessive, deeply weathered unit that forms a broad annular valley around Mount Jukes.||Mount Jukes Intrusive Complex|||Relatively homogeneous coarse-grained quartz gabbro.|
14021|Neranleigh-Fernvale beds|22845|6|Mentioned|p46|Early Carboniferous|Late Devonian|||||||
14021|Neranleigh-Fernvale beds|23799|6|Mentioned|p8, p122|||Of the South D'Aguilar and Beenleigh Subprovinces.||||||
14021|Neranleigh-Fernvale beds|23811|5|Briefly described|Map Legend|Visean|Tournaisian|Feldspathic and lithic meta-arenite, metasiltstone, chert, jasper, metabasic volcanic rock, conglomerate.||||||20-DEC-04
14021|Neranleigh-Fernvale beds|23812|5|Briefly described|p15, p137|Early Carboniferous|Early Carboniferous|Geological Province: Clarence-Moreton Basin.||||||
14021|Neranleigh-Fernvale beds|24418|6|Mentioned|p11|||Metasediments.||||||30-JUN-06
14021|Neranleigh-Fernvale beds|37509|6|Mentioned|p504|||||||||
14021|Neranleigh-Fernvale beds|38307|6|Mentioned|Fig.1|||||||||
14021|Neranleigh-Fernvale beds|38805|6|Mentioned|p87|||||||||
14021|Neranleigh-Fernvale beds|39079|5|Briefly described|p6|||||||||
14021|Neranleigh-Fernvale beds|39943|6|Mentioned|Table 10A|||||||||
14021|Neranleigh-Fernvale beds|39998|5|Briefly described|p189|||||||||
14021|Neranleigh-Fernvale beds|40475|6|Mentioned|p3|||||||||
14021|Neranleigh-Fernvale beds|40484|6|Mentioned|p63|||||||||
14021|Neranleigh-Fernvale beds|40623|5|Briefly described|p6|||||||||
14021|Neranleigh-Fernvale beds|40780|4|Described|p5|||||||||
14021|Neranleigh-Fernvale beds|40787|5|Briefly described|p346|||||||||
14021|Neranleigh-Fernvale beds|40896|6|Mentioned|p10|||||||||
14021|Neranleigh-Fernvale beds|40960|6|Mentioned|p215|||||||||
14021|Neranleigh-Fernvale beds|41822|6|Mentioned|p240|||||||||
14021|Neranleigh-Fernvale beds|41906|3|Fully described|Table 1 p11|||||||||23-NOV-15
14021|Neranleigh-Fernvale beds|41917|6|Mentioned|Fig.3 P528|||||||||
14021|Neranleigh-Fernvale beds|42316|6|Mentioned|p17|||||||||
14021|Neranleigh-Fernvale beds|42317|4|Described|p2|||||||||
14021|Neranleigh-Fernvale beds|42336|4|Described|p2|||||||||
14021|Neranleigh-Fernvale beds|42619|5|Briefly described|p29|||||||||
14021|Neranleigh-Fernvale beds|42669|5|Briefly described|p234|||||||||
14021|Neranleigh-Fernvale beds|42901|5|Briefly described|Fig.12 P412|||see also Fig.11 P411||||||
14021|Neranleigh-Fernvale beds|42970|6|Mentioned|p116|||||||||
14021|Neranleigh-Fernvale beds|43076|5|Briefly described|p4|||||||||
14021|Neranleigh-Fernvale beds|43092|5|Briefly described|p20|||||||||
14021|Neranleigh-Fernvale beds|43161|5|Briefly described|14||Carboniferous|||||||
14021|Neranleigh-Fernvale beds|44093|5|Briefly described|p242 App. 1|Carboniferous|Devonian|In the Beenleigh Block. Geological Province: New England Fold Belt.||||||
14021|Neranleigh-Fernvale beds|60079|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Meta-arenite, metasiltstone, chert, jasper, basic metavolcanics, conglomerate.||||||
14021|Neranleigh-Fernvale beds|60993|5|Briefly described|p17|Paleozoic|Paleozoic|Unconformably overlain by the Marburg Subgroup units.||||||07-NOV-08
14021|Neranleigh-Fernvale beds|61775|5|Briefly described|p181||Early Carboniferous|Comprise greywacke, argillite and chert that have undergone low grade regional metamorphism. Interpreted as the upper part of an accretionary prism.||||||06-MAY-13
14021|Neranleigh-Fernvale beds|63779|6|Mentioned|p1140|Carboniferous|Devonian|||||||
14021|Neranleigh-Fernvale beds|65380|5|Briefly described|p658, 660-663, 665-667, 671-672, 676-679|||Beenleigh Block, D'Aguilar Block. Detrital zircons from granitic sources in this unit may be considerably older than depositional age. Sample from Mt Nebo gives 351 +/-2 Ma detrital zircon age. Maximum depositional age from detrital zircon: 332 +/-3 Ma|||||Includes sandstones.|
14021|Neranleigh-Fernvale beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Beenleigh and South D'Aguilar Subprovinces.||||||
14021|Neranleigh-Fernvale beds|68679|3|Fully described|p321-322, p331, p333-336, p386, p392|Tournaisian|Tournaisian|See also p393 Fig.5.74, p394, p427, p433, p451. Fleming et al. (1974) and Korsch and Harrington (1981). Previously the Neranleigh-Fernvale Group of Bryan and Jones (1950); they combined the upper two units of the Brisbane Schists (Denmead, 1928): the Neranleigh Series and the Fernvale Series. The name Neranleigh itself was first used by Rands (1889) combining Neranwood (village) with Beenleigh (town). South D'Aguilar Subprovince, northern New England Orogen. The type area is the valley of Moggill Creek, W of Brisbane. Includes rocks in the Beenleigh Subprovince, from SE Brisbane to near Byron Bay. Upper plate accretionary assemblage. Deformation described in some detail. Other ages given. RELATED UNITS (continued): Correlated with the Texas beds. Possibly equivalent to Amamoor beds. Is intruded by Enoggera Granite, Samford and Mount Samson Granodiorites.|351 +/- 2 Ma (Korsch et al., 2009).|||Adjoins and partly faulted against Bunya Phyllite. Is faulted against and unconformably underlies Northbrook beds. Is overlain unconformably by Brisbane Tuff and Ipswich Coal Measures. See COMMENTS.|A heterogeneous succession of sandstone (commonly volcanolithic and locally oolitic), siltstone, chert and minor mafic volcanics (including pillow basalt), conglomerate and jasper; low greenschist metamorphosed. Fossils are rare.|
14021|Neranleigh-Fernvale beds|69599|6|Mentioned|p594|||||||Is overlain unconformably by the Oxley Group.||
14021|Neranleigh-Fernvale beds|69952|5|Briefly described|p38, p42|Carboniferous|Devonian|||||Is overlain unconformably by Brisbane Tuff. Is intruded by Enoggera Granite and Samford and Mount Samson Granodiorites.||
14021|Neranleigh-Fernvale beds|70125|5|Briefly described|p398|Carboniferous|Devonian|Beenleigh Block. Zircon ages described in some detail.||||||
14032|Netherwood Tonalite|23032|5|Briefly described|p21,24|Early Silurian|Early Ordovician|||||||
14032|Netherwood Tonalite|23424|5|Briefly described|Table 8.1 p332.|Early Silurian|Early Ordovician|Intrudes Judea Formation. Two plutons. The eastern one is overlain by the Graveyard Creek Group, therefore age is early Ordovician to early Silurian. I-Type. Graveyard Creek Subprovince.||||||
14032|Netherwood Tonalite|23431|5|Briefly described|p541|||||||||
14032|Netherwood Tonalite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 77. I-Type.||||||
14032|Netherwood Tonalite|41260|5|Briefly described|p35|||Reserved as Netherwood Quartz Diorite||||||
14032|Netherwood Tonalite|41679|6|Mentioned|Fig.2|||||||||
14032|Netherwood Tonalite|41719|2|Defined|p215|Early Silurian|Ordovician|||||||
14032|Netherwood Tonalite|41739|6|Mentioned|Fig.2|||||||||
14032|Netherwood Tonalite|41740|6|Mentioned|p222|||||||||
14032|Netherwood Tonalite|42054|6|Mentioned|p273|||||||||
14032|Netherwood Tonalite|42693|5|Briefly described|map legend|Ordovician||||||||
14032|Netherwood Tonalite|42933|3|Fully described|p51|||||||||
14032|Netherwood Tonalite|43259|4|Described|Appendix 1,p20.|Early Silurian|Early Ordovician|||||||
14032|Netherwood Tonalite|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
14032|Netherwood Tonalite|43480|6|Mentioned|26|||||||||
14032|Netherwood Tonalite|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Broken River Province/Graveyard Creek Subprovince. Presented informally as Netherwood tonalite.||||||11-APR-07
14032|Netherwood Tonalite|67848|5|Briefly described|p3 Fig.2, p4, p14, p15.|Ordovician|Ordovician|Part of basement to Camel Creek Subprovince. Plutonic phases of an incipient arc assemblage.||||Intrudes Judea Formation.||
14032|Netherwood Tonalite|68336|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||||Biotite-hornblende tonalite.|
14032|Netherwood Tonalite|68341|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|Graveyard Creek Subprovince.|||||Biotite-hornblende tonalite.|
14032|Netherwood Tonalite|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Broken River Province. This unit is mapped with the Saddington Tonalite under the same symbol, Ogr.||||||
14032|Netherwood Tonalite|69030|5|Briefly described|p6|Ordovician|Ordovician|Graveyard Creek Subprovince (Broken River Province).||||Intrudes Judea Formation.||
14032|Netherwood Tonalite|69592|5|Briefly described|p251 Fig.4.35, p253-256, p258-259|Early Ordovician|Early Ordovician|Withnall (1993). Broken River Province. Forms two small, partially fault-dismembered plutons. Geochemical plots.||||Is overlain nonconformably by Graveyard Creek Group. Intrudes Donaldsons Well Volcanic Member and is in contact with the turbidites in the Judea Formation.|Fine- to medium-grained biotite-hornblende tonalite to quartz diorite, showing variable alteration and no internal strain.|
14041|New Cannindah Conglomerate Member|30451|5|Briefly described|p27|||||||||
14041|New Cannindah Conglomerate Member|31586|5|Briefly described|p6|||Fauna||||||
14041|New Cannindah Conglomerate Member|31587|6|Mentioned|p60|||Lithostrotion distribution. See also P67||||||
14041|New Cannindah Conglomerate Member|42547|4|Described|p51|||||||||
14041|New Cannindah Conglomerate Member|44360|2|Defined|p1,10-12,21,25,30,32||Visean|Map. Member of Dakiel Formation.||||||
14068|Newberry Metamorphic Group|22533|6|Mentioned|p55|Mesoproterozoic|Mesoproterozoic|In Georgetown Region||||||
14068|Newberry Metamorphic Group|22780|5|Briefly described|map|Mesoproterozoic|Mesoproterozoic|||||||12-JAN-05
14068|Newberry Metamorphic Group|22781|3|Fully described|p11|Proterozoic|Proterozoic|Yambo Province||||||
14068|Newberry Metamorphic Group|22811|5|Briefly described|p597, Fig.2 p598|Mesoproterozoic|Paleoproterozoic|of Yambo Subprovince. Max age: Late Palaeoproterozoic.||||||07-NOV-08
14068|Newberry Metamorphic Group|23420|4|Described|p 143- 144 table 4.4||Paleoproterozoic|Also see p120. In the Coen Inlier of the Yambo Subprovince. Age: <1638 +/- 15Ma. Previously described as Dargalong Group on the basis of it's similarity with the Yambo Metamorphic Group.||||||26-FEB-14
14068|Newberry Metamorphic Group|23429|5|Briefly described|p440|||Also see Fig 13.18 p440.||||||
14068|Newberry Metamorphic Group|23430|5|Briefly described|p450|||||||||
14068|Newberry Metamorphic Group|24485|5|Briefly described|p26|||Geological Province: Yambo Subprovince||||||
14068|Newberry Metamorphic Group|42610|6|Mentioned|p4|||Reserved as Newberry Metamorphics.||||||
14068|Newberry Metamorphic Group|42650|5|Briefly described|p13|||Supersedes in part Coen Metamorphics east and north east of Coen||||||
14068|Newberry Metamorphic Group|42765|5|Briefly described|p18|||||||||
14068|Newberry Metamorphic Group|43287|6|Mentioned|Map Legend||Paleozoic|||||||07-NOV-08
14068|Newberry Metamorphic Group|43596|4|Described|p6 Fig. 6, p14, p20 Tb. 1||Mesoproterozoic|Comprises 3 gniess units: Kimba, Kitja and Penny Genisses. Part of Yambo Province, together with Yambo Metamorphic Group. Interpreted to be faulted against the Yambo Metamorphic Group.||||||26-FEB-14
14068|Newberry Metamorphic Group|43665|4|Described|p10||Proterozoic|||||||
14068|Newberry Metamorphic Group|43738|5|Briefly described|p5||Proterozoic|||||||
14068|Newberry Metamorphic Group|43820|5|Briefly described|Map Legend||Mesoproterozoic|||||||
14068|Newberry Metamorphic Group|63866|5|Briefly described|p76, p79-p80, p85|Calymmian|Calymmian|Yambo Subprovince, Coen Region. Numeric age is interpreted to represent the age of the precursor to a gneiss of this group.|1564 +/- 12 Ma (SHRIMP, Black, OZCHRON)||||High-grade (upper amphibolite-granulite) metamorphic rocks.|
14068|Newberry Metamorphic Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Etheridge Province.||||||
14068|Newberry Metamorphic Group|69591|5|Briefly described|p61, p70, p71 Fig.2.69, p72, p76-77|Paleoproterozoic|Paleoproterozoic|Coen Inlier, Etheridge Province. Similar to Yambo Metamorphic Group. Is poorly exposed along an elongate 30km wide belt along the SE side of Coen Inlier.|||Kimba, Kitja and Penny Gneisses.||Upper amphibolite to granulite grade metamorphic rocks including quartzite, amphibolite, orthogneiss, paragneiss, schist and mafic granulite.|
14068|Newberry Metamorphic Group|69592|6|Mentioned|p241|Mesoproterozoic|Mesoproterozoic|Coen Inlier. Has detrital ages around 1580-1477 Ma.||||||
14068|Newberry Metamorphic Group|70207|6|Mentioned|p74|Mesoproterozoic|Paleoproterozoic|||||||
14068|Newberry Metamorphic Group|70345|6|Mentioned|p3|Mesoproterozoic|Palaeoproterozoic|||||||
14068|Newberry Metamorphic Group|70673|6|Mentioned|p7|||Age range given as Paleoproterozoic-Mesoproterozoic.||||||
14068|Newberry Metamorphic Group|71592|5|Briefly described|Appendix A.|||Etheridge Province.|1639+/-12 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
14068|Newberry Metamorphic Group|71792|3|Fully described|p3-p5|Mesoproterozoic|Paleoproterozoic|Yambo Subprovince, Etheridge Province. Outcrops along the eastern margin of the Coen Inlier and is assumed to be the basement to the Savannah Province. Rocks previously assigned to the Coen Metamorphic Group east of the Macrossan Fault have been reassigned to this group. Named for Mount Newberry on the Ebagoola 1:250k map sheet. Forms a belt 30km wide covering 1500 km2. This group has a strong north to northeasterly magnetic fabric. Crystallisation age is derived from an unpublished GA Geochron delivery.|1564 +/- 12 Ma (crystallisation age)||Includes the Penny Gneiss, Kimba Gneiss and the Kitja Gneiss.|Intruded by the Buthen Buthen Granite.|Amphibolite, garnet muscovite-biotite schist associated with granite, sillimanite-mica schist, gneiss and quartzite.|
14068|Newberry Metamorphic Group|71849|5|Briefly described|p8, p79, p98, p195|Mesoproterozoic|Paleoproterozoic||||Penny Gneiss.|Is intruded by McIlwraith and Lankelly Granites.||
14068|Newberry Metamorphic Group|71854|5|Briefly described|Map legend.|Mesoproterozoic|Paleoproterozoic||||Kitja Gneiss, Penny Gneiss.|||
14068|Newberry Metamorphic Group|73387|6|Mentioned|p33|||Etheridge Province.||||||
14123|Nicholson Granite Complex|22673|6|Mentioned|64|||Geological province: Mount Isa Basin.||||||14-NOV-06
14123|Nicholson Granite Complex|22680|6|Mentioned|85|||||||||
14123|Nicholson Granite Complex|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14123|Nicholson Granite Complex|23405|6|Mentioned|p565|||||||||
14123|Nicholson Granite Complex|23406|6|Mentioned|p608|||Parts contained as clasts in the Fish River Formation.||||||16-JUN-09
14123|Nicholson Granite Complex|24419|5|Briefly described|p17, p18|Paleoproterozoic|Paleoproterozoic|Includes the Cliffdale Volcanics.  Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
14123|Nicholson Granite Complex|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14123|Nicholson Granite Complex|31421|6|Mentioned|p507|||||||||
14123|Nicholson Granite Complex|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|35950|6|Mentioned|p304|||||||||
14123|Nicholson Granite Complex|36012|3|Fully described|Table 1|||See also p8.||||||14-NOV-06
14123|Nicholson Granite Complex|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|37462|5|Briefly described|p234|||||||||
14123|Nicholson Granite Complex|38042|6|Mentioned|Fig.1|||||||||
14123|Nicholson Granite Complex|38237|6|Mentioned|p130|||||||||
14123|Nicholson Granite Complex|38335|6|Mentioned|p1727|||||||||
14123|Nicholson Granite Complex|38584|4|Described|p4|||||||||
14123|Nicholson Granite Complex|38900|6|Mentioned|p66|||||||||
14123|Nicholson Granite Complex|39123|6|Mentioned|p157|||||||||
14123|Nicholson Granite Complex|39445|5|Briefly described|Table 2|||See also p38.||||||14-NOV-06
14123|Nicholson Granite Complex|39685|6|Mentioned|Fig.1|||||||||
14123|Nicholson Granite Complex|39925|6|Mentioned|p337|||||||||
14123|Nicholson Granite Complex|40489|6|Mentioned|p88|||Also Mention on p89.||||||14-NOV-06
14123|Nicholson Granite Complex|40491|6|Mentioned|p79|||||||||
14123|Nicholson Granite Complex|40840|6|Mentioned|Map legend|||||||||
14123|Nicholson Granite Complex|41125|6|Mentioned|p35|||||||||
14123|Nicholson Granite Complex|41319|6|Mentioned|p195|||||||||
14123|Nicholson Granite Complex|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
14123|Nicholson Granite Complex|41721|3|Fully described|p4|||Includes the Norris and Nicholson granites of Roberts et al (1963). Comprises non-equigranular, coarse- to medium-grained hornblende and/or biotite-bearing granite, adamellite and granodiorite.||||||01-AUG-07
14123|Nicholson Granite Complex|41722|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
14123|Nicholson Granite Complex|41757|4|Described|p207|||||||||
14123|Nicholson Granite Complex|42754|6|Mentioned|p3|||||||||
14123|Nicholson Granite Complex|43595|6|Mentioned|p353|||Rb-Sr date: 1804+/-83 Ma.||||||14-NOV-06
14123|Nicholson Granite Complex|45162|6|Mentioned|p11|||||||||
14123|Nicholson Granite Complex|45166|5|Briefly described|p8|||||||||
14123|Nicholson Granite Complex|46804|6|Mentioned|p154|||||||||
14123|Nicholson Granite Complex|49001|2|Defined|p1|Carpentarian|Carpentarian|||||||
14123|Nicholson Granite Complex|49002|6|Mentioned|p1|||||||||
14123|Nicholson Granite Complex|61936|5|Briefly described|p193, p194 Fig. 6|||Geological Province: Lawn Hill Platform, Eastern Fold Belt, Mount Isa Inlier.||||||
14123|Nicholson Granite Complex|65228|5|Briefly described|p20.|Orosirian|Orosirian|SE McArthur Basin. Felsic; geochemically similar to Scrutton Volcanics. Ages from different phases of the granite (Page et al. 2000).|1856 +/- 3 Ma; 1845 +/- 3 Ma.|||Intrudes Murphy Metamorphic complex.||
14123|Nicholson Granite Complex|65232|5|Briefly described|p9, p8 Fig. 7|||Comagmatic I-type granitoids intrude Murphy Metamorphics. Age: 1856 Ma, 1845 Ma. Biotite +/- muscovite granite and hornblende-biotite granodiorite. Geol Prov: Murphy Inlier. See also Nicholson Granite, p67-68.||||||09-FEB-10
14123|Nicholson Granite Complex|65337|6|Mentioned|p50.||||||||K-feldspar rich granite.|
14123|Nicholson Granite Complex|66529|5|Briefly described|p20 Fig.7, p21  |||Also shortened to Nicholson Granite on p20.|~1840 Ma (M. Ahmad, NTGS, pers.comm.)|||Intrudes the Murphy Metamorphics and Cliffdale Volcanics.|Biotite +/-  muscovite granite and hornblende-biotite granodiorite.|
14123|Nicholson Granite Complex|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p29|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Nicholson Igneous Event. Informally subdivided into 6 or 7 units. See also Nicholson Granite (p9).|1845 +/- 3 Ma.|Nicholson Suite.||Intrudes Cliffdale Volcanics.|Xenolithic porphyritic hornblende-biotite and biotite granite, microgranite, greisen.|
14123|Nicholson Granite Complex|68998|5|Briefly described|vi, p34-37|||Murphy Province. This name is used interchangeably with Nicholson Granite. Contains inherited grains aged up to c.2500 Ma, matching the detrital spectrum of the Murphy Metamorphics. This age determination substantiates the "Barramundi" age commonly assumed for granites in the Murphy Province. Most outcrops are moderately to deeply weathered. Intruded by microgranite dykes. Additional ages are derived from Page et al (2000) and include 1856 +/- 3 Ma and 1845 +/- 3 Ma (SHRIMP U-Pb).|1846 +/- 6 Ma (magmatic crystallisation).|||Intrudes (cross-cuts) the Murphy Metamorphics.|Deeply weathered, deep red to white, generally megacrystic (feldspar phenocrysts to 10cm) felsic granite.|30-JUN-20
14123|Nicholson Granite Complex|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Murphy Orogen.||||Intrudes Murphy Metamorphics.||12-JUL-16
14123|Nicholson Granite Complex|69418|6|Mentioned|p3:21|||Murphy Province. Hosts the Crystal Hill greisen Sn-W deposit (described).||||||12-JUL-16
14123|Nicholson Granite Complex|69423|4|Described|p8:1, 3-5|Orosirian|Orosirian|Sweet and Slater (1975), Ahmad and Wygralak (1989). Murphy Inlier, Murphy Province. Comagmatic with Connellys and Cliffdale Volcanics. Eight lithological varieties (Gardner, 1978) were simplified into two groups by Ahmad (1987). SHRIMP U-Pb zircon ages of two samples. Hosts copper and several small tin +/- tungsten occurrences (eg Crystal Hill).|1856 +/- 3 Ma & 1845 +/- 3 Ma (Page et al., 2000)||Norris, Nicholson Granites.|Intrudes Murphy Metamorphics.|Group A: inequigranular, coarse- to medium-grained hornblende- and/or biotite-bearing granite, quartz monzonite and granodiorite; common mafic xenoliths and K-feldspar phenocrysts. Group B: equigranular quartz monzonite, granite and alkali granite.|12-JUL-16
14123|Nicholson Granite Complex|69430|5|Briefly described|p15:11, 49-51|||Appears as Nicholson Granite in the text as often as it appears as Nicholson Granite Complex in diagrams.||||Is overlain unconformably by Westmoreland Conglomerate (Tawallah Group).|Includes hornblende-biotite granodiorite and biotite-muscovite granite.|12-JUL-16
14123|Nicholson Granite Complex|69433|5|Briefly described|p18:2|||Probable source of 1847 +/- 13 Ma sediment (zircons) for Wire Creek Sandstone.||||Is overlain unconformably by Wire Creek Sandstone.||12-JUL-16
14123|Nicholson Granite Complex|69434|6|Mentioned|p19:1, 4|||Murphy Inlier. A source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||||12-JUL-16
14123|Nicholson Granite Complex|69591|5|Briefly described|p30-31, p60|||Camooweal-Murphy Domain. Is coeval with the Kalkadoon Granodiorite to the S.|1845 +/- 3 Ma (Geoscience Australia unpub. data).|||Intrudes Cliffdale Volcanics.|Xenolithic porphyritic hornblende-biotite and biotite granite, microgranite, greisen.|
14123|Nicholson Granite Complex|69673|6|Mentioned|p3|||||||||
14123|Nicholson Granite Complex|70849|5|Briefly described|Map legend.|Orosirian|Orosirian|Murphy Province.||||Intrudes Murphy Metamorphics and Cliffdale Volcanics.|Hornblende-biotite adamellite and granodiorite, medium- to coarse-grained, inequigranular. Biotite + muscovite granite and adamellite, medium- to fine-grained, equigranular.|
14123|Nicholson Granite Complex|71369|6|Mentioned|p47|||Basement rocks of the South Nicholson Basin.||||||
14123|Nicholson Granite Complex|71592|5|Briefly described|Appendix A.|||Murphy Region.|1846+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
14123|Nicholson Granite Complex|72526|5|Briefly described|p8 Fig.1.3.|Orosirian|Orosirian|3 U-Pb SHRIMP igneous crystallisation ages given. Shown as being located in the west and central part of the South Nicholson Basin and the Southeastern McArthur Basin. See also South Nicholson Granite Complex p6.|1845+/-3 Ma, 1856+/-6 Ma|||Probably overlain by Westmoreland Conglomerate and Wire Creek Sandstone.||
14123|Nicholson Granite Complex|72912|5|Briefly described|p5 Fig.3.|Orosirian|Orosirian|Located in the west part of the South Nicholson Basin and the Southeastern McArthur Basin. Three U-Pb zircon igneous crystallisation ages (Ma) shown. See also Nicholson Granite p19.|1856 +/- 6 Ma to 1845 +/- 3 Ma.|||Shown as overlying Cliffdale Volcanics, Murphy Metamorphics. Unconformably underlies Westmoreland Conglomerate.||
14123|Nicholson Granite Complex|72919|4|Described|p1, p4-9, p11, p93|Orosirian|Orosirian|Murphy Province, North Australian Craton. Two varieties have been described; Group A, a coarse- to medium-grained massive porphyritic hornblende +/-biotite granite-granodiorite, characterised by large K-feldspar crystals and abundant mafic xenoliths, and Group B, characterised as an equigranular biotite +/-muscovite granite-adamellite with rare hornblende and xenoliths. New U-Pb SHRIMP zircon magmatic crystallisation age of 1855 +/- 5 Ma. Previously reported geochronology yielded ages of 1856 +/- 3 Ma, 1845 +/- 3 Ma, and 1846 +/- 6 Ma (Page et al., 2000; Kositcin et al., 2013). Broadly coeval with Connellys Volcanics and Cliffdale Volcanics.|1855 +/- 5 Ma U-Pb SHRIMP|||Intrudes Murphy Metamorphics.|Includes biotite granite, coarse- to medium-grained massive porphyritic granite-granodiorite, and equigranular granite-adamellite.|
14123|Nicholson Granite Complex|73042|6|Mentioned|p4|Orosirian|Orosirian|Southern McArthur Basin and South Nicholson Basin region. Geochronology is a U-Pb zircon igneous crystallisation age.|1856+/-6 Ma, 1845+/-3 Ma, 1846+/-6 Ma|||||
14123|Nicholson Granite Complex|73427|6|Mentioned|p3|Orosirian|Orosirian|North Australian Craton, Murphy Inlier.|1855-1845 Ma|||||
14148|Nimbin Rhyolite|22582|4|Described|p69||Tertiary|Lamington Volcanics. Overlies Lismore Basalt, overlain by Blue Knob Basalt||||||
14148|Nimbin Rhyolite|24299|6|Mentioned|p184|||||||||
14148|Nimbin Rhyolite|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14148|Nimbin Rhyolite|30604|1|Redefined|p69|Cenozoic|Cenozoic|||||||19-NOV-08
14148|Nimbin Rhyolite|30605|6|Mentioned|p268|||early Miocene?||||||
14148|Nimbin Rhyolite|30687|6|Mentioned|p65|||Tertiary age. See also p64, Miocene age.||||||
14148|Nimbin Rhyolite|31130|6|Mentioned|Fig. 2|||Correlation. Early Miocene.||||||
14148|Nimbin Rhyolite|32924|6|Mentioned|p113|||Refers McTaggart (1961)||||||
14148|Nimbin Rhyolite|34092|5|Briefly described|p11|||||||||
14148|Nimbin Rhyolite|34340|6|Mentioned|Table 6.1|||||||||
14148|Nimbin Rhyolite|34593|6|Mentioned|p540|||||||||
14148|Nimbin Rhyolite|35050|6|Mentioned|p130|||||||||
14148|Nimbin Rhyolite|35296|4|Described|p13|||See also P12.||||||
14148|Nimbin Rhyolite|36056|6|Mentioned|p31|||||||||
14148|Nimbin Rhyolite|36411|6|Mentioned|p269|||Refs.Duggan & Mason 1978 for redefinition.||||||
14148|Nimbin Rhyolite|36806|6|Mentioned|p131|||||||||
14148|Nimbin Rhyolite|40623|5|Briefly described|p39|||||||||
14148|Nimbin Rhyolite|40896|4|Described|p8|||||||||
14148|Nimbin Rhyolite|43161|4|Described|13|||||||||
14148|Nimbin Rhyolite|43881|1|Redefined|p6-7,49,55-58,63,154||Tertiary|Inc.Minyon Falls Rhyolite Mbr,Boomerang Ck.Obsidian Mbr,Dorroughby Tuff Mbr:inc in MacPherson Volcs.||||||
14148|Nimbin Rhyolite|44818|6|Mentioned|p275|||||||||
14148|Nimbin Rhyolite|45018|14|Not recorded|p38|||(Urbenville)||||||
14148|Nimbin Rhyolite|48917|6|Mentioned|p38|||Stratigraphy||||||
14148|Nimbin Rhyolite|69599|5|Briefly described|p640|||Tweed volcano, centred on Mount Warning.||||Approximate equivalent of Binna Burra and Springbrook Rhyolites in QLD.|Peraluminous or high-silica rhyolite.|
14148|Nimbin Rhyolite|73581|5|Briefly described|p6|||Tweed Volcano. Overlies Beechmont Basalt/Lismore Basalt. Underlies Hobwee Basalt/Blue Knob Basalt.|||||Rhyolitic tuff and rhyolite lavas up to 100 m thick.|
14173|Ninmaroo Formation|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Dolostone, limestone, (ooid, petoidal and echinoderm grainstone, cryptalgal boundstone, flat pebble conglomerate), dolomitic sandstone.  Overlies Georgina Limestone.||||||21-JUN-04
14173|Ninmaroo Formation|8217|5|Briefly described|Map Legend|Ordovician|Cambrian|Dolomite, minor limestone-crystalline dolostone, algal boundstone, grainstone.||||||
14173|Ninmaroo Formation|10116|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Dolomite, micrite, grainstones, conglomerate, boundstones, limestone, sandstone.||||||
14173|Ninmaroo Formation|12891|5|Briefly described|p733 Fig. 2|Early Ordovician|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
14173|Ninmaroo Formation|12951|5|Briefly described|p143 fig 4, p145 fig 6, p148|Early Ordovician|Late Cambrian|Georgina Basin.||||Tomahawk beds interfingers.||
14173|Ninmaroo Formation|13995|5|Briefly described|p75-76, p79|||Druce et al. (1982). Georgina Basin. Contains rostroconches (listed) in beds of Datsonian (latest Cambrian) age, and a tentative nautiloid.||||||
14173|Ninmaroo Formation|22646|6|Mentioned|p 104|Early Ordovician|Early Ordovician|Georgina Basin||||||
14173|Ninmaroo Formation|22954|4|Described|Fig1p6,p10-1,17-8|Warendan|Payntonian|Consists of Unbunmaroo, Jiggamore, Mort, Corrie and Datson Members.||||||30-JAN-07
14173|Ninmaroo Formation|23553|5|Briefly described|p2276|Ordovician|Cambrian|Geological Province: Georgina Basin.||||||
14173|Ninmaroo Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 1000m.||||||
14173|Ninmaroo Formation|24334|5|Briefly described|p48 Tb.1|Arenig|Middle Cambrian|Age: 500-485 Ma. Formation is Fmn. in text. Geological Privince: Georgina Basin.||||||20-NOV-06
14173|Ninmaroo Formation|24442|5|Briefly described|p45|Ordovician|Cambrian|Interfingers with Tomahawk Formation.||||||
14173|Ninmaroo Formation|30479|6|Mentioned|p16|||Ordovician age. See also Fig.3||||||
14173|Ninmaroo Formation|30598|6|Mentioned|p50|||||||||
14173|Ninmaroo Formation|31287|6|Mentioned|p424|||||||||
14173|Ninmaroo Formation|31572|4|Described|Fig. 1|||L.Ord.||||||
14173|Ninmaroo Formation|32576|6|Mentioned|p50|||Potential aquifer||||||
14173|Ninmaroo Formation|32952|4|Described|p1188|||Ordovician. See also pp92 and 93.||||||20-NOV-06
14173|Ninmaroo Formation|33111|4|Described|p39|||||||||
14173|Ninmaroo Formation|33482|2|Defined|Fig.4||Ordovician|||||||
14173|Ninmaroo Formation|33657|6|Mentioned|p1|||||||||
14173|Ninmaroo Formation|34252|6|Mentioned|Po.10|||Fossils||||||
14173|Ninmaroo Formation|34287|6|Mentioned|p76|||||||||
14173|Ninmaroo Formation|34454|5|Briefly described|Table 2|||Cambrian - Ordovician||||||
14173|Ninmaroo Formation|34847|6|Mentioned|Table 1 P31|||Stratigraphy and hydrocarbon prospects.||||||20-NOV-06
14173|Ninmaroo Formation|35032|6|Mentioned|p117|||||||||
14173|Ninmaroo Formation|35121|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|35139|4|Described|Table.2|||||||||
14173|Ninmaroo Formation|35146|6|Mentioned|p469|||||||||
14173|Ninmaroo Formation|35936|6|Mentioned|p614|||||||||
14173|Ninmaroo Formation|36234|3|Fully described|p169|||See also Fig.1.||||||
14173|Ninmaroo Formation|36243|6|Mentioned|Table 1A|||||||||
14173|Ninmaroo Formation|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
14173|Ninmaroo Formation|36580|6|Mentioned|Fig.3|||||||||
14173|Ninmaroo Formation|36645|6|Mentioned|p312|||||||||
14173|Ninmaroo Formation|37572|4|Described|p161|||See also p162 and Figs.7 and 8.||||||20-NOV-06
14173|Ninmaroo Formation|38444|5|Briefly described|p106|||||||||
14173|Ninmaroo Formation|38446|5|Briefly described|p152|||||||||
14173|Ninmaroo Formation|38532|4|Described|p231|||||||||
14173|Ninmaroo Formation|38608|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14173|Ninmaroo Formation|39445|5|Briefly described|Table 4|||See also p61, p64 andFig.5. Included Georgina Lst on map.||||||20-NOV-06
14173|Ninmaroo Formation|39690|6|Mentioned|Fig.2|||||||||
14173|Ninmaroo Formation|39921|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Late Cambrian to Early Ordovician||||||
14173|Ninmaroo Formation|39943|6|Mentioned|Table 2B|||||||||
14173|Ninmaroo Formation|40127|6|Mentioned|p8|||||||||
14173|Ninmaroo Formation|40136|5|Briefly described|p34|||||||||
14173|Ninmaroo Formation|40810|5|Briefly described|p14|||||||||
14173|Ninmaroo Formation|40830|6|Mentioned|p12|||||||||
14173|Ninmaroo Formation|40852|6|Mentioned|Fig.3.7|||||||||
14173|Ninmaroo Formation|40906|6|Mentioned|Fig.11|||||||||
14173|Ninmaroo Formation|41524|6|Mentioned|Fig.3|||||||||
14173|Ninmaroo Formation|42058|6|Mentioned|p115|||||||||
14173|Ninmaroo Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||20-NOV-06
14173|Ninmaroo Formation|42060|6|Mentioned|Fig.5 P140|||||||||
14173|Ninmaroo Formation|42354|6|Mentioned|p9|Datsonian||In the Georgina Basin.||||||20-NOV-06
14173|Ninmaroo Formation|42643|6|Mentioned|p32|||Georgina Basin||||||
14173|Ninmaroo Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
14173|Ninmaroo Formation|43807|6|Mentioned|Fig.2,p347|||||||||
14173|Ninmaroo Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
14173|Ninmaroo Formation|44091|14|Not recorded|p17,Tb.1,p19,21||Late Cambrian|Trempealeauan.||||||
14173|Ninmaroo Formation|44121|14|Not recorded|p5|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|44210|14|Not recorded|p7|||||||||
14173|Ninmaroo Formation|44212|2|Defined|p110,112|||||||||
14173|Ninmaroo Formation|44233|14|Not recorded|Fig.1|Early Ordovician|Late Cambrian|U.Camb-L.Ord.||||||
14173|Ninmaroo Formation|44273|14|Not recorded|Map Legend||Early Ordovician|||||||
14173|Ninmaroo Formation|44276|2|Defined|p20,27,Tb.2|||||||||
14173|Ninmaroo Formation|44291|14|Not recorded|p7|||||||||
14173|Ninmaroo Formation|44308|14|Not recorded|p5,10,Tb.1|Late Carboniferous|Tremadocian|||||||
14173|Ninmaroo Formation|44309|2|Defined|Tb.1,p9-12,16-7,map|Ordovician|Cambrian|Rests disconformably on Georgina Limestone and Mungerebar Limestone.||||||20-NOV-06
14173|Ninmaroo Formation|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
14173|Ninmaroo Formation|44312|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44326|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44351|14|Not recorded|p15|||||||||
14173|Ninmaroo Formation|44358|6|Mentioned|p10|||||||||
14173|Ninmaroo Formation|44361|14|Not recorded|Map Legend|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44362|4|Described|p10,Tb.1|Ordovician|Cambrian|||||||
14173|Ninmaroo Formation|44457|2|Defined|p.8, Tb.1, map|Early Ordovician|Late Cambrian|Upper Cambrian-L.Ord. SANDOVER RIVER map (F53-8).||||||20-NOV-06
14173|Ninmaroo Formation|44458|5|Briefly described|map legend|Early Ordovician|Late Cambrian|Grey dolomite, algal dolomite; pelletal dolarenite, quartzose, with some ooltihs; some sandstone and siltstone.||||||16-NOV-04
14173|Ninmaroo Formation|44469|2|Defined|p.9, Tb.I|||(F53-12). See also p.8,12-14,16. Tb.II. Overlies Arrinthrunga Fm. Laterally equivalent to lower part of Tomahawk Beds. Fossils; good aquifers.||||||30-JAN-07
14173|Ninmaroo Formation|44470|5|Briefly described|map legend|||Upper Cambrian - Lower Ordovician.||||||02-DEC-04
14173|Ninmaroo Formation|44543|2|Defined|p32-34,46|Early Ordovician|Late Cambrian|Overlies Chatsworth Limestone. Name changed from Ninmaroo Limestone to Ninmaroo Formation as dolomite becomes as prevelant as limestone and some sandstone occurs to the west of Glenormiston.||||||30-JAN-07
14173|Ninmaroo Formation|44620|14|Not recorded|p88||Tremadocian|Conodonts.||||||
14173|Ninmaroo Formation|44852|14|Not recorded|p71||Early Ordovician|||||||
14173|Ninmaroo Formation|44882|14|Not recorded|p265,287||Tremadocian|In French||||||
14173|Ninmaroo Formation|44920|14|Not recorded|Map Legend, Sheet 4|Early Ordovician|Late Cambrian|||||||
14173|Ninmaroo Formation|45002|14|Not recorded|p16,24|||Late Cambrian fossils.||||||
14173|Ninmaroo Formation|45051|5|Briefly described|p6|||Upper Cambrian - Ordovician. See also p1,4,10.||||||20-NOV-06
14173|Ninmaroo Formation|45052|2|Defined|p18|Ordovician|Cambrian|Cambrian - Ordovician||||||
14173|Ninmaroo Formation|45058|6|Mentioned|p8|||See also P23. Correlation with Pander Greensand.||||||
14173|Ninmaroo Formation|45079|6|Mentioned|p12|||Map legend on p12.||||||20-NOV-06
14173|Ninmaroo Formation|45094|3|Fully described|p11|||||||||
14173|Ninmaroo Formation|45115|6|Mentioned|p6|||||||||
14173|Ninmaroo Formation|45130|6|Mentioned|p3|||||||||
14173|Ninmaroo Formation|45166|5|Briefly described|Table 15|||||||||
14173|Ninmaroo Formation|45168|6|Mentioned|Table 1, P6|||||||||
14173|Ninmaroo Formation|46887|6|Mentioned|p251|||||||||
14173|Ninmaroo Formation|46897|6|Mentioned|p351|||See also Fig.2||||||
14173|Ninmaroo Formation|46956|6|Mentioned|p160|||||||||
14173|Ninmaroo Formation|46958|4|Described|p183|||||||||
14173|Ninmaroo Formation|46959|6|Mentioned|Table 1|||||||||
14173|Ninmaroo Formation|47024|6|Mentioned|p1|||||||||
14173|Ninmaroo Formation|47057|6|Mentioned|p554|||||||||
14173|Ninmaroo Formation|48901|14|Not recorded|Not recorded||Early Ordovician|L.Ordovician.||||||
14173|Ninmaroo Formation|48906|14|Not recorded|Tb.1,App.D|||||||||
14173|Ninmaroo Formation|48971|6|Mentioned|p42|||||||||
14173|Ninmaroo Formation|49027|4|Described|p12|||||||||
14173|Ninmaroo Formation|50100|5|Briefly described|p22|Early Ordovician|Early Ordovician|Comprises micritic limestone, intraformational breccia, dolomite, chert, mudstone and minor cross-stratified dolomitic limestone; highly fossiliferous.  Overlain by Swift Formation.||||||30-JAN-07
14173|Ninmaroo Formation|50244|5|Briefly described|p88, p89 Fig. 1, p90, p92 Fig. 3, p95|Ordovician|Cambrian|Includes; Datson, Corrie, Mort, Jiggamore and Unbunmaroo Members. Geological Province: Georgina Basin. Dolomitic. On p100 Fig. 7 also.||||||
14173|Ninmaroo Formation|60122|3|Fully described|p4-5, p24-25|Early Ordovician|Late Cambrian|Supersedes N. Limestones and N.Series (Whitehouse 1936). Includes 5 formal members not recognised in TOBERMORY. Conformable over Chatsworth Lst (absent in TOBERMORY); disconformable over Arrinthrunga Fm; interfingers with Tomahawk Fm. Max. thick: 795m.||||||19-MAY-05
14173|Ninmaroo Formation|60123|4|Described|p5|Ordovician|Cambrian|Limestone, dolostone, minor quartz sandstone. Disconformably underlies Austral Downs Limestone. Disconformably overlies: Arrinthrunga Formation. Thickness: 795m.||||||28-APR-05
14173|Ninmaroo Formation|60359|5|Briefly described|Map Legend|Ordovician|Cambrian|Calcarenite, calcilutite, breccia, limestone, marl.||||||
14173|Ninmaroo Formation|60590|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Dolostone, limestone, minor quartz sandstone.  Time equivalent of Tomahawk Formation.  Overlies the Arrinthrunga Formation; overlain by Kelly Creek Formation.||||||25-NOV-04
14173|Ninmaroo Formation|60675|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Dolostone, limestone, minor quartz sandstone.||||||
14173|Ninmaroo Formation|61404|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Cockroach Group. Dolostone, limestone, minor quartz sandstone. Geological Province: southern Georgina Basin.||||||
14173|Ninmaroo Formation|62793|6|Mentioned|p272|Early Ordovician|Late Cambrian|The C. lindstromi Assemblage Zone 8 occupies an interval from 404 to 563 m above the base of Ninmaroo Formation, defining the base of the Ordovician in the Black Mountain section.|||Includes Unbunmaroo Member.|Overlies Chatsworth Limestone.||21-MAR-12
14173|Ninmaroo Formation|63450|4|Described|p76, p78 Fig. 5, p82, p83|Ordovician|Late cambrian|Conformable on Chatsworth Lst (Burke River Struct.Belt), unconformable on Arrinthrunga Fm. in W. Toko Syncline, on Georgina Fm.in E. Overlain by Swift Fm (karstified); and by Kelly Ck. Fm. Max .thickness: 950m. In Georgina Basin, East Toko Syncline.||||||07-FEB-11
14173|Ninmaroo Formation|64068|4|Described|pp72-73, p69, 71, 75, p8, 19|Early Ordovician|Late Cambrian|795 m thick in type section. Paleopoles from this and other units define a major change in APWP. Conformably and gradationally overlies and may interdigitate with Chatsworth Limestone. Laterally interdigitates with Tomahawk Formation. Conformably to disconformably overlain by Kelly Creek Formation. Formerly (Prichard 1960) included rocks now in Kelly Creek Formation.||Of Cockroach Group.|Includes Unbunmaroo, Jiggamore, Mort, Corrie and Datson Members.|Disconformably overlies Georgina Limestone, Mungerebar Limestone, Arrinthrunga Fm. Conformably overlain by Swift Formation.|Mixed-lithology limestones, dolostones; minor quartz sandstone, conglomerate. Surficial manganocrete.|05-APR-12
14173|Ninmaroo Formation|64443|6|Mentioned|p18||Late Cambrian|||||Disconformably overlies Arrinthrunga Formation.||14-MAY-14
14173|Ninmaroo Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
14173|Ninmaroo Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin. Lateral equivalent is the Tomahawk beds.||||||11-FEB-09
14173|Ninmaroo Formation|65489|5|Briefly described|p123, p125-127|Ordovician|Cambrian|Georgina Basin. Contains traces of bitumen.||||Overlies Chatsworth Limestone (conformably), and Arrinthrunga Formation and Georgina Limestone (unconformably). Is overlain by Kelly Creek Formation.||
14173|Ninmaroo Formation|67028|6|Mentioned|p371 Tb. 5|Devonian|Cambrian|Listed with Chatswood Limestone, magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|398-495 Ma magnetic age range|||||10-AUG-15
14173|Ninmaroo Formation|67323|5|Briefly described|GIS attrib tbl, p83, p90, p92 Fig.12.2|Ordovician|Cambrian|See also Solid Geology Map. Georgina Basin. Appears as Nimaroo Formation on p83.||Cockroach Group.||Unconformably overlies Arrinthrunga Formation and Georgina Limestone; overlies Chatsworth Limestone conformably. Is overlain by Kelly Creek Formation and Swift Formation.|Calcarenite, dolomite, limestone, oolitic and algal limestone, calcilutite.|
14173|Ninmaroo Formation|67402|5|Briefly described|p25, p25 tbl RRM3, p165 tbl LPB1|Bendigonian|Late Cambrian|Georgina Basin, Toko Syncline. Maximum thickness of 950m. Potential carbon dioxide storage reservoir, sealed by the Nora Formation. Gas has been observed in fractures from this unit. Deposited in sub-tidal to supra-tidal environments. See also p213 fig GRG3, p213 fig GRG5, p214, p215, p217.||||Unconformably overlies the Arrinthrunga Formation. Overlain by the Kelly Creek Formation.|Predominantly limestone.|
14173|Ninmaroo Formation|67870|6|Mentioned|p39, p43|Ordovician|Cambrian|Georgina Basin.||||||
14173|Ninmaroo Formation|69377|5|Briefly described|map legend|Early Ordovician|Late Cambrian|||Cockroach Group|||Calcarenite and dolomite, oolitic and algal limestone and calcilutite|
14173|Ninmaroo Formation|69437|5|Briefly described|p22:10, 15|Early Ordovician|Cambrian|Southern Georgina Basin. Hosts surficial manganocrete and pisolitic manganiferous lag.||||Overlies Arrinthrunga Formation. Is overlain by Kelly Creek Formation.||12-JUL-16
14173|Ninmaroo Formation|69443|3|Fully described|p28:7, 19, 25-27, 44|Early Ordovician|Late Cambrian|Casey (1959) after Whitehouse (1936). Southern Georgina Basin. Forms extensive tracts of smooth rounded hills to isolated low rises. Has five Members in the type section in BOULIA map area (Shergold and Druce, 1980), but these have not been identified in the NT. Up to 795m thick (in the type section). Contains a diverse fossil fauna (listed). Interdigitates with Tomahawk Formation. Open to restricted marine and emergent evaporitic carbonate sedimentation. Contains numerous sedimentary structures. Has returned locally significant manganese assay results.||Cockroach Group.||Overlies Chatsworth Limestone conformably and Arrinthrunga Formation, Georgina or Mungereba Limestones disconformably. Is overlain by Swift or Kelly Creek Formations.|Ooid, peloid, bioclast, intraclast, microbial and mixed-lithology limestone and dolostone; minor quartz sandstone and conglomerate. Microbial carbonate rocks include microbial dololaminite, stromatolitic doloboundstone and stromatolitic biostromes.|12-JUL-16
14173|Ninmaroo Formation|69458|6|Mentioned|p42:20|||||||Is overlain by Austral Downs Limestone.||14-SEP-18
14173|Ninmaroo Formation|69561|6|Mentioned|p33 fig 2|Datsonian|Payntonian|||||||
14173|Ninmaroo Formation|69591|3|Fully described|p87, p91, p93-94|Ordovician|Cambrian|Widespread unit in SE Georgina Basin. Deposited on a regional unconformity, except in the Burke River Structural Belt. Whitehouse (1936) included the thick succession of limestone at Black Mountain, Mount Ninmaroo and Mount Datson as Ninmaroo Limestone; Casey (1959) separated the lower part of the Black Mountain section as the Chatsworth Limestone, and renamed the remainder the Ninmaroo Formation to recognise the varied lithologies elsewhere. Up to 950m thick; thins westwards. Contains a rich and varied fauna (listed). Upper part is laterally equivalent to the Swift Formation which unconformably overlies it locally.||Cockroach Group.||Overlies Mungerebar, Georgina Limestones disconformably, Mount Birnie beds unconformably, and Chatsworth Limestone conformably (diachronous boundary). Conformably underlies Kelly Creek Formation.|Limestone (including oolitic, algal and echinodermal) and dolomite banks with marly, shaly, sandy and brecciated interbeds.|
14173|Ninmaroo Formation|69673|4|Described|p114 fig 92, p117, p118, p135|Ordovician|Cambrian|795m thick. Fossils includes conodonts which are the basis for age constraints. Some reservoir potential.||Cockroach Group||Conformably overlain by Kelly Creek Formation, overlies Chabalowe Formation, Arrinthrunga Formation|Ooid, peloid, bioclast, intraclast, microbial limestone and dolostone with minor quartz sandstone and conglomerate.|
14173|Ninmaroo Formation|70380|5|Briefly described|p745-746, p758-759|Tremadocian|Furongian|Southern Georgina Basin. Contains a conodont fauna very similar to that collected in Oolloo Dolostone in the Claravale area, leading to reappraisal of the age of the latter unit. Is lithologically similar to, and of an equivalent age to, the Florina Formation (Daly Basin).||||Interdigitates with Tomahawk Formation.||
14173|Ninmaroo Formation|70749|6|Mentioned|p54|||Georgina Basin, Centralian Superbasin.||Cockroach Group.||||
14173|Ninmaroo Formation|71284|5|Briefly described|p489, p492|||Black Mountain area, western Queensland.|||Unbunmaroo Member.|||
14173|Ninmaroo Formation|72297|5|Briefly described|p747-748|||Georgina Basin.|||||Includes dolomite; where exposed at the surface, is karstified.|
14173|Ninmaroo Formation|72516|6|Mentioned|p94|Ordovician|Cambrian|HAY RIVER map sheet. Georgina Basin.||||Equivalent to the Tomahawk Formation.||09-JUN-21
14173|Ninmaroo Formation|73083|6|Mentioned|p75|Early Ordovician|Late Cambrian|||||Underlain by Camooweal Dolostone.||
14207|Nogo beds|23037|4|Described|p10,40-8,91,2,7,15,115|Late Permian|Late Carboniferous|Replaces some sections of the Goonambula Granodiorite.||||||
14207|Nogo beds|23042|6|Mentioned|p8|||||||||
14207|Nogo beds|41246|6|Mentioned|Map legend|Permian||||||||
14207|Nogo beds|43008|5|Briefly described|map legend|||||||||
14207|Nogo beds|43017|5|Briefly described|Fig.3,p375|||||||||
14207|Nogo beds|50598|5|Briefly described|Map Legend|Early Permian|Early Permian|Basaltic to andesitic volcanic sandstone, conglomerate and breccia, andesite lava, ignimbrites.||||||
14207|Nogo beds|60282|6|Mentioned|p4|||||||||
14207|Nogo beds|61087|5|Briefly described|Map Legend|Early Permian|Early Permian|Basaltic to andesitic volcanic sandstone and oligomictic conglomerate or breccia, andesite lava and subordinate flow-banded rhyolite and dacitic to rhyolitic ignimbrite; locally cleaved siltstone, carbonaceous mudstone and minor sandstone.||||||
14207|Nogo beds|61777|5|Briefly described|p224, p228||Early Permian|Geological Province: Yarrol Province. May be correlatives of Camboon Volcanics. See p228 for more info. Volcanic sandstone and oligomictic conglomerate are common rock type.||||||07-FEB-11
14207|Nogo beds|64398|5|Briefly described|Map legend|Early Permian|Early Permian|Basaltic to andesitic volcanic sandstone and oligomictic conglomerate or breccia, andesite lava and subordinate flow-banded rhyolite and dacitic to rhyolitic ignimbrite; locally cleaved siltstone, carbonaceous mudstone and minor sandstone.||||||18-AUG-08
14207|Nogo beds|64399|5|Briefly described|Map legend|Early Permian|Early Permian|Overlain by Cynthia beds; overlies Lorray Fm. Basaltic to andesitic volc.sst + oligomictic conglom.or breccia, andesite lava, subordinate flow-banded rhyolite and dacitic to rhyolitic ignimbrite; locally cleaved siltst., carbonaceous mudst. + minor sst||||||19-AUG-08
14207|Nogo beds|64855|6|Mentioned|p29|Early Permian|Early Permian|||||||22-FEB-10
14207|Nogo beds|65388|3|Fully described|p39-43; p35, 36, 37, 114, 314, 329|Early Permian|Late Devonian|Nogo Subprovince, Yarrol Province. Of Whitaker and others (1974). Designated a type locality in a road cutting along the Eidsvold-Cracow road, adjacent to the Burnett River crossing. Includes areas previously mapped as Coonambulla Granodiorite. Consists of two distinct geochemical suites; the high-Ti suite, could be equivalent to Late Devonian basalts in the Three Moon Conglomerate; The low-Ti suite is probably Permian. Intruded by unnamed gabbros and diorites. Intermediate to basic lavas and volcaniclastic rocks, lithic arenite, cleaved mudstone, chert and conglomerate. Probably correlate with Narayen beds  and Owl Gully Volcanics, and in part with Camboon Volcanics. See also p439, 447.||||||
14207|Nogo beds|68008|6|Mentioned|p139|||||||May be partial time equivalent of Owl Gully Volcanics.||
14207|Nogo beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Auburn Subprovince. This unit, with the Narayen and Smoky beds, and the Yaparaba Volcanics, are all mapped under the symbol, Pvy.||||||
14207|Nogo beds|68679|5|Briefly described|p312-313, p343-344, p351-353, p397, p408|Permian|Permian|See also p416, p419. Whitaker et al. (1974). Nogo Subprovince (Camboon Volcanic Arc), Yarrol Province, northern New England Orogen. Outcrop area of ~350 km2 between the Rawbelle Batholith and Mulgildie Basin. Thickness unknown. Much of the unit is strongly hornfelsed by the Eidsvold Complex and Rawbelle Batholith. Poorly preserved Permian marine fossils. Less robust correlations mentioned.||||Probably correlated with Narayen beds, Owl Gully Volcanics and part of Camboon Volcanics. Is intruded by Pollard Granodiorite.|Mainly andesite-derived volcaniclastic sandstone and oligomictic conglomerate; andesitic or basaltic lavas, flow-banded rhyolite and dacitic to rhyolitic ignimbrite; sparse fine-grained, cleaved siltstone, carbonaceous mudstone and minor sandstone.|
14207|Nogo beds|73450|6|Mentioned|p28|||||||Intruded by Boolgal Granophyre.||
14233|Noosa Quartz Diorite|23251|5|Briefly described|Table 5 p32|Cretaceous|Late Jurassic|Age: K/Ar dates at 142 and 146 Ma. Intrudes Tiaro Coal Measures. Bauple Province.||||||30-NOV-05
14233|Noosa Quartz Diorite|40623|5|Briefly described|p55|||||||||
14233|Noosa Quartz Diorite|43100|4|Described|p60|Cretaceous|Late Jurassic|||||||
14233|Noosa Quartz Diorite|44724|14|Not recorded|p59,Fig.4,p67,Pl.IV,|||p69,Plate V, p70,71.||||||
14233|Noosa Quartz Diorite|44752|14|Not recorded|p99||Late Jurassic|||||||
14233|Noosa Quartz Diorite|44783|14|Not recorded|p41|||||||||
14233|Noosa Quartz Diorite|44928|5|Briefly described|Map Legend|Cretaceous|Jurassic|||||||
14233|Noosa Quartz Diorite|68553|6|Mentioned|Map legend|Cretaceous|Jurassic|This unit, as well as the Mount Bauple Syenite, Mount Urah Granodiorite, and unnamed intrusive units, are all mapped under the symbol, JKi.||||||
14233|Noosa Quartz Diorite|68679|6|Mentioned|p312|Cretaceous|Jurassic|Northern New England Orogen.||||||
14233|Noosa Quartz Diorite|69594|5|Briefly described|p560-563|Early Cretaceous|Late Jurassic|Whitsunday Volcanic Province. Well-exposed at Granite Bay, Noosa National Park (photographs). Appears as Nosa Quartz Diorite on p562. Geochronology by Evernden and Richards (1962) and Green and Webb (1974); other age determinations given.|~145 Ma (K-Ar: biotite and hornblende).|||Intrudes Myrtle Creek Sandstone.|Light grey, fine- to medium-grained quartz diorite. Locally intruded by leucogranite and aplite veins and contains numerous, locally aligned xenoliths.|
14233|Noosa Quartz Diorite|73450|6|Mentioned|p84|Cretaceous|Jurassic|||||||
14235|Nora Formation|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Limonitic coquina limestone, siltstone, sandstone.||||||
14235|Nora Formation|9394|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Geological Province: Georgina Basin. Siltstone, dolomite, oolitic ironstone, sandstone. Overlies Tomahawk beds.||||||21-NOV-06
14235|Nora Formation|9694|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Underlies Dulcie Sandstone. Overlies Tomahawk beds. Geological Province: Georgina Basin. Siltstone, dolomite, oolitic ironstone, sandstone.||||||21-NOV-06
14235|Nora Formation|10116|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Of the Toko Group. Siltstone, sandstone, limestone.||||||
14235|Nora Formation|12891|5|Briefly described|p733 Fig. 2|Middle Ordovician|Middle Ordovocian|Geological province: SW Georgina Basin.||||||07-FEB-11
14235|Nora Formation|12951|6|Mentioned|p143 fig 4, p145 fig 6|Middle Ordovician|Early Ordovician|Georgina Basin.||||||
14235|Nora Formation|13995|5|Briefly described|p67, p74, p76-77, p79-80, p83, p101-102|Ordovician|Ordovician|Georgina Basin. Comparatively shallow-water deposits. Three brachiopod genera are recorded, but are in need of reassessment. Contains Middle Ordovician pelecypods and gastropods, and nautiloids. Has a rich trilobite fauna (described).||||Part-equivalent to Stairway Sandstone.|Mainly interbedded siltstones, minor sandstones and limestones (coquinites).|
14235|Nora Formation|22646|6|Mentioned|p 105|Early Ordovician|Early Ordovician|In the Georgina Basin.||||||21-NOV-06
14235|Nora Formation|22954|6|Mentioned|Fig3p9|Ordovician|Ordovician|||||||
14235|Nora Formation|23214|5|Briefly described|p123|||Maggs (1963).||||||
14235|Nora Formation|23858|5|Briefly described|p924 Fig 8|Ordovician||||||||
14235|Nora Formation|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Georgina Basin.||||||
14235|Nora Formation|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Of Toko Group. Geological Province: Georgina Basin. Maximum thickness: 120m.||||||
14235|Nora Formation|24442|5|Briefly described|p49|||On TOBERMORY sheet.||||||
14235|Nora Formation|30983|5|Briefly described|p70|||||||||
14235|Nora Formation|31572|6|Mentioned|p21|||||||||
14235|Nora Formation|33657|6|Mentioned|p1|||||||||
14235|Nora Formation|33738|6|Mentioned|p54|||||||||
14235|Nora Formation|34252|6|Mentioned|Po.2|||Fossils.||||||21-NOV-06
14235|Nora Formation|34454|6|Mentioned|Table 2|||L.Ordovician||||||
14235|Nora Formation|34847|6|Mentioned|Table 1|||Stratigraphy and hydrocarbon prospects.||||||21-NOV-06
14235|Nora Formation|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
14235|Nora Formation|35139|4|Described|Table.2|||||||||
14235|Nora Formation|35146|6|Mentioned|p470|||||||||
14235|Nora Formation|36234|3|Fully described|p173|||||||||
14235|Nora Formation|36243|6|Mentioned|Table 1A|||||||||
14235|Nora Formation|36580|6|Mentioned|p469|||See also Fig.1||||||
14235|Nora Formation|37572|4|Described|p163|||See also p169 and Fig.8.||||||21-NOV-06
14235|Nora Formation|37727|6|Mentioned|Fig.1|||||||||
14235|Nora Formation|38832|6|Mentioned|p157|||||||||
14235|Nora Formation|39445|5|Briefly described|Table 4|||||||||
14235|Nora Formation|39921|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
14235|Nora Formation|39943|6|Mentioned|Table 2A|||||||||
14235|Nora Formation|40136|5|Briefly described|p34|||||||||
14235|Nora Formation|40538|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Siltstone; minor sandstone; oolitic ironstone. Geological Province: Georgina Basin.||||||15-NOV-05
14235|Nora Formation|40810|5|Briefly described|p14|||||||||
14235|Nora Formation|40855|6|Mentioned|p329|||||||||
14235|Nora Formation|40906|4|Described|p27|||Mention Fig.9||||||
14235|Nora Formation|41385|6|Mentioned|Fig.4|||||||||
14235|Nora Formation|41524|6|Mentioned|Fig.3|||||||||
14235|Nora Formation|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||21-NOV-06
14235|Nora Formation|42060|6|Mentioned|Fig.5 P140|||||||||
14235|Nora Formation|42354|6|Mentioned|p10|||||||||
14235|Nora Formation|42504|5|Briefly described|Table 54 P79|||||||||
14235|Nora Formation|43105|5|Briefly described|Fig.4,p9.|||||||||
14235|Nora Formation|43803|6|Mentioned|Fig.5,p71|||||||||
14235|Nora Formation|43808|5|Briefly described|p294|||||||||
14235|Nora Formation|44308|14|Not recorded|p10,Tb.1||Early Ordovician|Of Toko Group.||||||
14235|Nora Formation|44309|2|Defined|Tb.1,p7,12,17,19,map|||Conformably overlies Coolibah Formation.||||||
14235|Nora Formation|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
14235|Nora Formation|44326|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
14235|Nora Formation|44327|2|Defined|Tb.I,p.11,14-16,map|||(F53-11). Conformably overlies Tomahawk Beds.||||||21-NOV-06
14235|Nora Formation|44328|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44334|14|Not recorded|map legend||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44358|2|Defined|App.p18|Early Ordovician|Early Ordovician|See also p10, Tb.1. (Middle-Middle Ordovician).||||||31-MAR-09
14235|Nora Formation|44469|2|Defined|p.10, Tb.I|||(F53-12). See also p.12,13,15,16,Tb.II. Contains phosphatic beds. Fossils.||||||
14235|Nora Formation|44470|5|Briefly described|map legend||Ordovician|Middle Ordovician.||||||02-DEC-04
14235|Nora Formation|44852|14|Not recorded|p71||Ordovician|Middle Ordovician.||||||
14235|Nora Formation|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Middle Ordovician||||||
14235|Nora Formation|45052|2|Defined|p128|Middle Ordovician|Middle Ordovician|Unit of Toko Group.||||||
14235|Nora Formation|45115|6|Mentioned|p6|||||||||
14235|Nora Formation|45118|6|Mentioned|p2,3|||||||||
14235|Nora Formation|45148|6|Mentioned|Fig.4|||In the Georgina Basin.||||||21-NOV-06
14235|Nora Formation|45155|6|Mentioned|Fig.8|||||||||
14235|Nora Formation|46841|4|Described|p104|||Also mention p97.||||||21-NOV-06
14235|Nora Formation|46897|6|Mentioned|Fig.3|||||||||
14235|Nora Formation|46956|6|Mentioned|p160|||||||||
14235|Nora Formation|46959|6|Mentioned|Table 1|||||||||
14235|Nora Formation|47024|6|Mentioned|Table 1|||||||||
14235|Nora Formation|48844|2|Defined|p.50-3||Ordovician|On many pages. p.2,16,17,47,48,50-3, F.26,58,59-62,68,69, Pl.8. M.Ordovician. (F53-11).||||||
14235|Nora Formation|48901|14|Not recorded|Not recorded||Ordovician|Middle Ordovician.  Part of Toko Group.||||||21-NOV-06
14235|Nora Formation|49027|4|Described|p17|||||||||
14235|Nora Formation|50091|6|Mentioned|p407, p413 Tb. 1|||Panderodus nogamii (conodont) found  - in Toko Range area (Qld).  Geological Province: Georgina Basin.||||||04-NOV-04
14235|Nora Formation|60122|3|Fully described|p31-32, p10 Tb. 1, p28 Fig. 33|Early Ordovician|Early Ordovician|Of Toko Group. Conformable on Kelly Cr. and Coolibah Fms; conformable below Carlo Sst and unconformable below Poodyea Fm. Max. thick: 250m. Geol.Prov: Georgina Basin.||||||21-NOV-06
14235|Nora Formation|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological province: Georgina Basin.||||||
14235|Nora Formation|60590|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group.  Micaceous and glauconitic siltstone, claystone, sandstone, minor dolostone; basal coquinite.  Overlies the Coolibah Formation; overlain by Carlo Sandstone.||||||21-NOV-06
14235|Nora Formation|61404|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Of the Toko Group. Micaceous and glauconitic siltstone, claystone, sandstone, minor dolostone; basal coquinite. Geological Province: southern Georgina Basin.||||||
14235|Nora Formation|62794|6|Mentioned|p289, 298, p303, 336|Early Ordovician|Early Ordovician|Georgina Basin. Overlies Coolibah Formation. Likely correlation exists between basal Nora Formation and upper Horn Valley Siltstone in Amadeus Basin, based on trilobites.||||||
14235|Nora Formation|63450|4|Described|p78 Fig. 5, p82|Arenig|Arenig|Conformably overlies Coolibah Formation; overlain conformably by Carlo Sandstone. Max. thickness: 250m. Geological province: Georgina Basin, West Toko Syncline. Basal coquinite with remainder being siltstone, mudstone and sandstone with minor dolostone.||||||07-FEB-11
14235|Nora Formation|63562|6|Mentioned|p338 fig 3, p349, p352 fig 10|Early Ordovician|Early Ordovician|Of Georgina Basin.||||Overlies Kelly Creek Formation.|Siliciclastics.|
14235|Nora Formation|64068|3|Fully described|p77, 75, 78, p19|Middle Ordovician|Middle Ordovician|Very diverse fauna.||Of Toko Group.||Conformably overlies Coolibah and Kelly Creek Formations. Conformably overlain by Carlo Sandstone or unconformably by Dulcie Sandstone.|Thin-bedded micaceous and glauconitic siltstone, claystone, fine sandstone, minor dolostone; basal bioclast grainstone-rudstone.|04-APR-12
14235|Nora Formation|64778|6|Mentioned|p13|Ordovician|Ordovician|Dulcie Syncline, Southern Georgina Basin.||||||
14235|Nora Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
14235|Nora Formation|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
14235|Nora Formation|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
14235|Nora Formation|65489|5|Briefly described|p123, p125-126|Ordovician|Ordovician|Georgina Basin. Contains bitumen.||||Is overlain by Carlo Sandstone.||
14235|Nora Formation|67323|5|Briefly described|p81, p83, p90, p92 Fig.12.2|Early Ordovician|Early Ordovician|See also GIS attrib tbl, Solid Geology Map. Toko Syncline, Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Toko Group||Overlies Kelly Creek Formation unconformably and Coolibah Formation conformably. Is overlain by Carlo Sandstone.|Dolomite, siltstone, fine arenite.|
14235|Nora Formation|67402|4|Described|p25 tbl RRM3, p213 fig GRG3|Castlemanian|Chewtonian|Georgina Basin. Deposited in shallow subtidal to intertidal environment or offshore below wave base. Gas has been observed from fractures of this unit. Maximum thickness of 235m. See also p213 fig GRG5, p214, p215, p216, p217, p219.||||Is laterally equivalent to or conformably overlies the Coolibah Formation. Overlain by the Carlo Sandstone.|Basal coquinite with an upper section of siltstone, mudstone and sandstone with minor dolomite.|
14235|Nora Formation|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Coolibah Formation. Is overlain by Carlo Sandstone.||12-JUL-16
14235|Nora Formation|69443|4|Described|p28:7, 27-30|Middle Ordovician|Early Ordovician|Casey in Smith (1963). Southern Georgina Basin. A recessive unit, poorly exposed. 42-250m thick. Lower part is richly fossiliferous (fauna listed). Floian to early Darriwilian age.||Toko Group.||Conformably overlies Kelly Creek and Coolibah Formations. Is overlain conformably by Carlo Sandstone, or unconformably by Dulcie Sandstone.|Thinly bedded, micaceous and glauconitic siltstone, claystone, fine sandstone and minor dolostone, with a basal bioclast grainstone-rudstone. Some siliciclastic units are rippled and cross-laminated.|12-JUL-16
14235|Nora Formation|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
14235|Nora Formation|69591|4|Described|p87, p94-95|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Up to 120m thick. Contains a diverse fossil assemblage (listed).||Toko Group.||Overlies Coolibah Formation conformably and Kelly Creek Formation disconformably. Is overlain conformably and transitionally by Carlo Sandstone.|Sandstone and siltstone with thin grey limestone in the lower part, dark brown and grey limonitic limestone in the middle, succeeded by olive, yellow, purple and grey siltstones and green and brown fine glauconitic sandstones.|
14235|Nora Formation|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
14235|Nora Formation|69673|4|Described|p114 fig 92, p118, p119 fig 94, p128|Ordovician|Ordovician|250m thick.||Toko Group||Overlies Coolibah Formation, overlain by Carlo Sandstone|Siltstone, claystone, sandstone and minor dolostone with a basal bioclast grainstone-rudstone.|
14235|Nora Formation|70380|6|Mentioned|p745|Darriwilian|Darriwilian|Southern Georgina Basin.||||||
14235|Nora Formation|71800|6|Mentioned|p26 fig 3|Early Ordovician|Early Ordovician|Georgina Basin.||||Overlies the Kelly Creek Formation.||
14235|Nora Formation|72297|5|Briefly described|p748|||Forms suitable cap rocks in the Toko Syncline, Georgina Basin.|||||Siltstone and mudstone.|
14235|Nora Formation|72503|6|Mentioned|p28|||Georgina Basin, Toko Ranges, far western Queensland. Histiodella serrata [conodont?] is recognised from this unit (originally referred to as Histiodella sinuosa).||||||
14240|Noranside Limestone|22954|6|Mentioned|Fig3p9||Tertiary|||||||
14240|Noranside Limestone|31572|4|Described|Fig.|||Tertiary||||||
14240|Noranside Limestone|33086|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14240|Noranside Limestone|33111|4|Described|p43|||Mention P6.||||||
14240|Noranside Limestone|35121|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14240|Noranside Limestone|35139|4|Described|Table.2|||||||||
14240|Noranside Limestone|37607|5|Briefly described|p333|||||||||
14240|Noranside Limestone|39445|5|Briefly described|Table 14|||||||||
14240|Noranside Limestone|44122|14|Not recorded|Fig.48,p321|||||||||
14240|Noranside Limestone|44133|5|Briefly described|p190 Fig. 10.30|Pliocene|Pliocene|||||||
14240|Noranside Limestone|44222|14|Not recorded|p120|||||||||
14240|Noranside Limestone|44276|2|Defined|map,Tb.2|||||||||
14240|Noranside Limestone|44277|14|Not recorded|Map Legend||Tertiary|(On white Formation card)||||||
14240|Noranside Limestone|44291|2|Defined|Tb.1,opp.p6,10,map||Tertiary|||||||
14240|Noranside Limestone|44351|2|Defined|p12-16,19-27,Fig.13|||Overlies Marion Formation.||||||
14240|Noranside Limestone|44361|14|Not recorded|Map Legend||Tertiary|||||||
14240|Noranside Limestone|44362|4|Described|p13,Tb.1||Tertiary|||||||
14240|Noranside Limestone|44543|2|Defined|p35,36|||Overlies Wilgunya Formation. Fossils.||||||
14240|Noranside Limestone|45052|4|Described|p136|||Cainozoic||||||
14240|Noranside Limestone|45094|6|Mentioned|p14|||Tertiary||||||
14240|Noranside Limestone|46958|6|Mentioned|Fig.2|||||||||
14240|Noranside Limestone|48844|14|Not recorded|p.57|||||||||
14240|Noranside Limestone|50100|6|Mentioned|p23|Cenozoic|Cenozoic|||||||
14240|Noranside Limestone|61155|5|Briefly described|p16|Middle Miocene|Middle Miocene|Together with Austral Downs Limestone thickness is 35m. Geological Province: Georgina Basin.||||||
14240|Noranside Limestone|66131|6|Mentioned|p242 Fig.2, p245|Miocene|Miocene|Late Miocene. Boulia region. Closely resembles Doonbara Formation.||||||
14240|Noranside Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.||||Overlies and may interfinger with Marion Formation.|White lacustrine limestone with a chalcedony cap .|
14240|Noranside Limestone|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Austral Downs and Horse Creek Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
14240|Noranside Limestone|69377|5|Briefly described|map legend|Neogene|Paleogene||||||White lacustrine limestone with a chalcedony cap|
14240|Noranside Limestone|69599|5|Briefly described|p584, p599-601|Miocene|Miocene|Casey (1959); Casey et al. (1960) and others. Noranside Basin. Small outliers occur for ~70km to the N and 25km to the NE. Up to 30m thick. Lacustrine deposits, with possible groundwater input. Has Pliocene silcrete. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek and Austral Downs Limestones; and Mount Coley Sinter.||||Unconformably overlies the Wilgunya Subgroup. Locally overlies or interdigitates with Marion Formation. Correlated with Doonbara, Whitula and Poodyea Formations; see COMMENTS for more.|Thin basal limestone with reworked lateritised detritus, overlain by fine-grained pelletal limestone grading up into a thick silicified limestone.|
14246|Normanby Formation|12575|5|Briefly described|p781, p784 Table 1.|Permian|Permian|Occurs as small fault blocks in a narrow belt west of Cooktown. Structural inliers are pervasively cleaved by Hunter-Bowen Orogeny. Apatite fission track analyses, vitrinite reflectance data are detailed.|290-245 Ma.|||||
14246|Normanby Formation|22497|6|Mentioned|p105|Permian|Permian|||||||
14246|Normanby Formation|23423|4|Described|p304 Table 7.3||Permian|Also see p258-259. Overlying unit Dalrymple Sandstone (unconformable), McLean Basalt||||||
14246|Normanby Formation|23426|5|Briefly described|p401.|||||||||
14246|Normanby Formation|23430|4|Described|p517|||Also see page 504 Table 14.5||||||
14246|Normanby Formation|23431|5|Briefly described|p539|||||||||
14246|Normanby Formation|23511|5|Briefly described|Map Legend||Late Permian|||||||
14246|Normanby Formation|24080|5|Briefly described|p445 Fig. 4|Permian|Permian|Sandstone, shale, coal.  Max. thickness: >1000m.  Geological Province: Laura Basin.||||||
14246|Normanby Formation|24086|5|Briefly described|p312 Fig. 1|Late Permian|Late Permian|||||||
14246|Normanby Formation|24213|5|Briefly described|p776 Fig. 1|Permian|Early Permian|||||||
14246|Normanby Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
14246|Normanby Formation|33772|6|Mentioned|p11|||||||||
14246|Normanby Formation|34046|6|Mentioned|Table II|||||||||
14246|Normanby Formation|36172|6|Mentioned|Appendix|||||||||
14246|Normanby Formation|37115|6|Mentioned|Fig.1|||||||||
14246|Normanby Formation|37137|4|Described|p252|||Formerly Oaky Creek Coal Measures.||||||
14246|Normanby Formation|37575|4|Described|p179|||||||||
14246|Normanby Formation|37613|5|Briefly described|p247|||See also Fig.1||||||
14246|Normanby Formation|39252|6|Mentioned|Fig. 15|||||||||
14246|Normanby Formation|39445|5|Briefly described|Table 8|||See also Table 9||||||
14246|Normanby Formation|41569|6|Mentioned|p72|||||||||
14246|Normanby Formation|41775|6|Mentioned|p72|||||||||
14246|Normanby Formation|42187|6|Mentioned|p319|||||||||
14246|Normanby Formation|42369|3|Fully described|p39-42|||Name introduced in 1965, in its current form.||||||22-APR-09
14246|Normanby Formation|42474|5|Briefly described|p27|||Cooktown 1:100 000 sheet||||||
14246|Normanby Formation|42490|6|Mentioned|p54|||Cooktown area.||||||
14246|Normanby Formation|42637|5|Briefly described|p21|||||||||
14246|Normanby Formation|42648|5|Briefly described|p41|||||||||
14246|Normanby Formation|42658|6|Mentioned|p26|||||||||
14246|Normanby Formation|43070|5|Briefly described|p50|||||||||
14246|Normanby Formation|43083|6|Mentioned|p184|||Displays Permian vulcanism.||||||17-JUN-09
14246|Normanby Formation|43098|2|Defined|p24|Permian||||||||
14246|Normanby Formation|43665|6|Mentioned|p19||Permian|||||||
14246|Normanby Formation|43883|14|Not recorded|p18 Fig.4-3||Permian|||||||
14246|Normanby Formation|43896|14|Not recorded|Map Legend|||||||||
14246|Normanby Formation|43979|14|Not recorded|p65-67||Permian|||||||
14246|Normanby Formation|44293|14|Not recorded|Map Legend||Permian|||||||
14246|Normanby Formation|44294|2|Defined|Tb.2,p12,21,25-6,map|||Formerly called "Oaky Creek Coal Measures". Overlies Hodgkinson Formation. Underlies Dalrymple Sandstone.||||||
14246|Normanby Formation|45025|4|Described|p63-64||Late Permian|||||||
14246|Normanby Formation|50587|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Yates Supersuite.  Geological Province: Kennedy Province.  Rhyolitic ignimbrite, andesitic to basaltic lava and tuff, arenite, siltstone, mudstone, conglomerate..||||||07-JUL-04
14246|Normanby Formation|50596|5|Briefly described|Map Legend|Late Permian|Late Permian|Rhyolitic, andesitic and basaltic lava flows, pyroclastic and sedimentry deposits, minor coal.||||||
14246|Normanby Formation|50630|5|Briefly described|Map Legend|Late Permian|Early Permian|Rhyolite, breccia, basalt, andesite, mudstone, siltstone, conglomerate, arenite.||||||
14246|Normanby Formation|60425|3|Fully described|p39, p41 Tb. 3, p199|Late Permian|Middle Permian|Of Jack (1879a,b). Unconformably overlain by Dalrymple Sandstone (Laura Basin) and Mclean Basalt. Thickness: <1000m. Quartzose arenite, polymictic conglomerate etc - v. detailed lithology (p39, p42 Tb. 3)||||||07-FEB-11
14246|Normanby Formation|65114|5|Briefly described|p383 Tb.1|?Early Permian||Tectonic unit: Lakefield Basin tectonic unit||||||
14246|Normanby Formation|68553|6|Mentioned|Map legend|Permian|Permian|This unit, as well as the Agate Creek, Galloway and Mount Little Volcanic Groups; parts of the Featherbed and Scardons Volcanic Groups; the Julago, Little Fork, Mitchell River and Nychum Volcanics, and the Little River Coal Measures, are all mapped under the symbol, Pvk.||||||
14246|Normanby Formation|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|261 +/- 5 Ma (SHRIMP).|||Is intruded by Pieter Botte Supersuite.||
14246|Normanby Formation|69592|5|Briefly described|p230, p243, p249|Permian|Permian|First described (in the Oaky Creek area SW of Cooktown) by Jack (1879); formalised by Lucas and deKeyser (1965). Mainly preserved as narrow (<2km wide), elongate NNW- and NNE-trending in-faulted belts, W and S of Cooktown. Strata are steeply dipping, faulted and locally folded. Post-Tabberabberan Orogeny. Conglomerate clasts were derived from Hodgkinson Formation. Contains Permian plant fossils (Glossopteris) and tabulate coral (Thamnopora).|||||Massive rhyolite (lava and ignimbrite), andesite, basalt, andesitic to rhyolitic tuff and breccia, conglomerate, sandstone (in part volcaniclastic), siltstone, mudstone, carbonaceous mudstone, coal and impure limestone.|
14246|Normanby Formation|70207|6|Mentioned|p109|Permian|Permian|Rossville area.||||||
14246|Normanby Formation|72297|5|Briefly described|p697|Permian|Permian|SE margin of the Laura Basin. Contains coal in three small faulted outliers, ~29km W of Cooktown.||||||
14253|Normanton Formation|22747|6|Mentioned|p15|||||||||
14253|Normanton Formation|23065|5|Briefly described|4, 18|||Of Rolling Downs Group.  In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
14253|Normanton Formation|23425|4|Described|p378|||Of Rolling Downs Group. Underlain by Allaru Mudstone. In the Carpentaria Basin Province.||||||21-NOV-06
14253|Normanton Formation|23431|5|Briefly described|p543|||||||||
14253|Normanton Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24047|5|Briefly described|p11|Cretaceous|Cretaceous|Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group. Maximum thickness: 250m.  Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Carpentaria Basin.||||||
14253|Normanton Formation|30020|6|Mentioned|Fig.1|||||||||
14253|Normanton Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|30584|4|Described|Table 1|||Also mentioned p6.||||||21-NOV-06
14253|Normanton Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|31164|6|Mentioned|Fig. 1|||Refers Rivereau (1966).||||||
14253|Normanton Formation|31165|6|Mentioned|Table 1|||||||||
14253|Normanton Formation|31168|6|Mentioned|p10|||||||||
14253|Normanton Formation|31208|6|Mentioned|Fig. 7|||||||||
14253|Normanton Formation|31433|5|Briefly described|p6|||L.Cretaceous. Paralic||||||
14253|Normanton Formation|31434|3|Fully described|Table 1|||See also p8.||||||21-NOV-06
14253|Normanton Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32314|6|Mentioned|Fig. 4|||||||||
14253|Normanton Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
14253|Normanton Formation|32396|6|Mentioned|p8,9,18||Early Cretaceous|Shallow marine and paralic, correlated with Mackunda Formation.||||||
14253|Normanton Formation|33150|4|Described|p8|||L.Cret.||||||
14253|Normanton Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
14253|Normanton Formation|33175|6|Mentioned|p284|||||||||
14253|Normanton Formation|33176|6|Mentioned|p171|||||||||
14253|Normanton Formation|33177|5|Briefly described|Table 1|||||||||15-JUL-04
14253|Normanton Formation|33178|6|Mentioned|p11|||||||||
14253|Normanton Formation|33182|6|Mentioned|Fig.1|||L.Cret.||||||
14253|Normanton Formation|33183|3|Fully described|p227|||Name revised and restricted.||||||21-NOV-06
14253|Normanton Formation|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|33561|6|Mentioned|p102|||||||||
14253|Normanton Formation|33642|6|Mentioned|p144|||Named by Laing and Power (1959) in the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|33772|6|Mentioned|p13|||||||||
14253|Normanton Formation|33773|4|Described|Table 1|||See also p17.||||||21-NOV-06
14253|Normanton Formation|34356|6|Mentioned|p2|||See also p20,21,32. Lower Cretaceous.||||||21-NOV-06
14253|Normanton Formation|34811|4|Described|Table 1|||||||||
14253|Normanton Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|35811|5|Briefly described|Table 3|||||||||
14253|Normanton Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
14253|Normanton Formation|36012|3|Fully described|Table 5|||See also p18, 20.||||||21-NOV-06
14253|Normanton Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|37608|3|Fully described|Table 1|||||||||
14253|Normanton Formation|38143|6|Mentioned|p20|||||||||
14253|Normanton Formation|39211|5|Briefly described|p36|||Fossils. Age||||||
14253|Normanton Formation|39445|5|Briefly described|Table 11|||||||||
14253|Normanton Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14253|Normanton Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|40648|6|Mentioned|p12|||||||||
14253|Normanton Formation|41064|6|Mentioned|p62|||||||||
14253|Normanton Formation|41266|6|Mentioned|Fig.3|||||||||
14253|Normanton Formation|41307|6|Mentioned|p5|||See also p20.||||||21-NOV-06
14253|Normanton Formation|42061|5|Briefly described|p157|||See also Fig.11||||||
14253|Normanton Formation|42637|5|Briefly described|p11|||||||||
14253|Normanton Formation|43105|6|Mentioned|p16|||||||||
14253|Normanton Formation|43630|6|Mentioned|p70|||also fig.4||||||
14253|Normanton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
14253|Normanton Formation|44031|14|Not recorded|p3,Tb.1||Cretaceous|||||||
14253|Normanton Formation|44082|6|Mentioned|p18,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
14253|Normanton Formation|44112|6|Mentioned|p82||Cenomanian|||||||
14253|Normanton Formation|44251|14|Not recorded|p4||Albian|||||||
14253|Normanton Formation|44346|14|Not recorded|opp.p5|||Equivalent of Allaru Member of Wilgunya Formation.||||||
14253|Normanton Formation|44515|2|Defined|p28||Albian|Overlain by Lynd Formation. Correlated with Kamileroi Limestone. No fossils.||||||
14253|Normanton Formation|44656|2|Defined|p325,328,Fig.48,T.10||Albian|||||||
14253|Normanton Formation|44747|14|Not recorded|p5,8,9||Albian|Contains Magoura Member (lower) Wernadinga Siltstone Member (upper). (late Albian)||||||
14253|Normanton Formation|44807|4|Described|p8-10,map||Early Cretaceous|||||||
14253|Normanton Formation|45004|14|Not recorded|p.8,14,15,28|||||||||
14253|Normanton Formation|45145|3|Fully described|Table 5|||See also p25 and Table 4.||||||21-NOV-06
14253|Normanton Formation|46791|6|Mentioned|Table 2|||||||||
14253|Normanton Formation|46872|6|Mentioned|p105|||||||||
14253|Normanton Formation|46937|6|Mentioned|Fig.10|||||||||
14253|Normanton Formation|49010|6|Mentioned|Fig.4|||In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|49011|6|Mentioned|Fig.3|||In the Carpentaria Basin.||||||21-NOV-06
14253|Normanton Formation|50044|6|Mentioned|p197|||Mentioned only as a time equivalent in the Gulf of Carpentaria region.||||||
14253|Normanton Formation|62837|5|Briefly described|Stratigraphic columns|Cenomanian|Cenomanian|Of the Rolling Downs Group.  Age: ~94-~91Ma. Geological Province: Carpentaria, Bamaga and Karumba Basins.||||||01-MAR-10
14253|Normanton Formation|64820|5|Briefly described|pS6 Fig. 4, pS9|Cenomanian|Albian|Top unit of Rolling Downs Group. Underlies the bauxite of the Bulimba Formation. Med.-fine-grained glauconitic sandstone with carbonaceous intercalated phases, and siltstone. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||27-AUG-18
14253|Normanton Formation|66529|6|Mentioned|p12 Fig.5, p16  |||Carpentaria Basin.||Unit in Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|66915|5|Briefly described|p6 Fig.3|Late Cretaceous|Early Cretaceous|Carpentaria Basin.||||||
14253|Normanton Formation|67323|5|Briefly described|GIS attrib tbl,  p86-87, p94 Fig.12.4|Cretaceous|Cretaceous|See also Solid Geology Map. Eromanga/Carpentaria Basins. Marginal-marine sediments.||||Overlies Allaru Mudstone.|Labile sandstone, siltstone, minor mudstone and cone-in-cone limestone.|
14253|Normanton Formation|67402|5|Briefly described|p177 tbl CRP/KRM1, p181|Cenomanian|Cenomanian|Carpentaria Basin. Deposited in a paralic to shallow marine environment. Approximately 150m thick.||||Overlies the Allaru Mudstone. Overlain by the Bulimba Formation.|Glauconitic sandstone and siltstone.|
14253|Normanton Formation|67784|5|Briefly described|p26|Albian|Albian|Carpentaria Basin. Age infered from Aptian belemnites and ammonites in underlying Wallumbilla Fm||Wilgunya Subgroup.||Overlies Allaru Mudstone.||27-AUG-18
14253|Normanton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Carpentaria Basin.||Unit in Rolling Downs Group.||Conformably overlies Polland Waterhole Shale.||
14253|Normanton Formation|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|68821|6|Mentioned|p292 Fig.1|Cretaceous|Cretaceous|Lower Cretaceous age.||Of the Rolling Downs Group.||||
14253|Normanton Formation|69297|5|Briefly described|p273, p274 fig 4. 3|Upper Cretaceous|Upper Jurassic|||Rolling Downs Group||Overlies the Allaru Mudstone.|Lithic glauconitic sandstones.|
14253|Normanton Formation|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|||||Is correlated with the onshore Yirrkala Formation.||12-JUL-16
14253|Normanton Formation|69582|6|Mentioned|p22|Upper Cretaceous|Upper Cretaceous|Eromanga Basin. Deposited in a paralic, fluvial and lacustrine environment.||||Overlies the Allaru Mudstone.||
14253|Normanton Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Allaru Formation. Is overlain unconformably by Armraynald Beds.||
14253|Normanton Formation|69594|5|Briefly described|p518, p521-522, p574|Cenomanian|Aptian|Youngest deposits in the Carpentaria Basin. Upper marine to paralic deposits. Thins markedly from NE to S and W. Faunal control on age limits discussed.||Rolling Downs Group.||Conformably overlies Allaru Mudstone.||
14253|Normanton Formation|69599|5|Briefly described|p601|Cretaceous|Cretaceous|One of the hosts of the world's largest deposit of bauxite on the west coast of Cape York. Formation of the bauxite discussed.||Rolling Downs Group.|||Medium- to fine-grained glauconitic sand with common carbonaceous intercalations; deeply weathered with a typical lateritic profile containing loose, free-running pisoliths of bauxite with little or no matrix.|
14253|Normanton Formation|71863|6|Mentioned|p4-p5|Cenomanian|Albian|Carpentaria Basin. Deposited during a marine incursion.||Rolling Downs Group||||
14253|Normanton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Carpentaria Basin.||Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|72799|6|Mentioned|p27|||||||||
14253|Normanton Formation|73083|6|Mentioned|p51, p54, p56, p62, p65, p68|Cretaceous|Cretaceous|Carpentaria Basin, Canobie Depression.||Rolling Downs Group|||Includes sandstone and conglomerate.|
14253|Normanton Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
14253|Normanton Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Partial aquifer. Capped by an unconformity.||Rolling Downs Group||Underlain by Allaru Mudstone.||
14253|Normanton Formation|73147|5|Briefly described|p129||Albian|||Rolling Downs Group.||Overlies Allaru Mudstone.||
14253|Normanton Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
14289|Northbrook beds|22845|6|Mentioned|p11  Fig6||Permian|||||||
14289|Northbrook beds|22846|6|Mentioned|p44||Permian|||||||
14289|Northbrook beds|23440|6|Mentioned|p150|||||||||
14289|Northbrook beds|23799|6|Mentioned|p125|||Probable equivalent of Cressbrook Creek Group.||||||
14289|Northbrook beds|39079|5|Briefly described|p6|||||||||
14289|Northbrook beds|39252|5|Briefly described|p22|||||||||
14289|Northbrook beds|40051|4|Described|p6|||||||||
14289|Northbrook beds|40623|6|Mentioned|Fig.31|||Mention Table 2||||||
14289|Northbrook beds|41917|6|Mentioned|Fig.3 P528|||||||||
14289|Northbrook beds|43008|5|Briefly described|map legend|||||||||
14289|Northbrook beds|43009|5|Briefly described|Map Legend|||||||||
14289|Northbrook beds|44925|5|Briefly described|Map Legend||Permian|||||||
14289|Northbrook beds|63779|6|Mentioned|p1138|Early Permian|Early Permian|Geological Province: Esk Trough.||||||
14289|Northbrook beds|63821|5|Briefly described|p19|Middle Permian|Middle Permian|Geological Province: Esk Trough.||||||07-FEB-11
14289|Northbrook beds|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with the Marumba and Cambroon beds; the Cedarton Volcanics, and the Kandanga Creek Megabreccia, are all mapped under the symbol, Pn.||||||
14289|Northbrook beds|68679|5|Briefly described|p321, p324, p326, p384-387, p389, p470|Guadalupian|Guadalupian|Campbell (1960), and others listed. Cressbrook Basin, northern New England Orogen; previously included in the Esk Basin. Cover basin sediments; ~1500m thick. Shallow-marine unstable shelf or slope environment; soft-sediment deformation; mass-flow deposits. Correlative with Cressbrook Creek Group.||||Is faulted against and unconformably overlies Jimna Phyllite, Neranleigh-Fernvale beds, Rocksberg Greenstone. Is faulted against and unconformably underlies Toogoolawah Group, Mount Byron Volcanics.|Andesitic tuff, minor dacitic flows and tuff interbedded with sandstone and mudstone in central areas; conglomerate (with abundant andesite and minor rhyolite clasts), sandstone, massive siltstone and massive chert.|
14289|Northbrook beds|73450|6|Mentioned|p107|||||||||
14311|Norwood Mudstone Member|33367|6|Mentioned|p26|||||||||
14311|Norwood Mudstone Member|33371|2|Defined|p58|Jurassic|Jurassic|Pt.of Westbourne Fm.||||||
14311|Norwood Mudstone Member|37995|6|Mentioned|p69|||||||||
14311|Norwood Mudstone Member|45110|5|Briefly described|p98|||||||||
14311|Norwood Mudstone Member|63218|6|Mentioned|p211.|||||Unit in Westbourne Formation.||||
14311|Norwood Mudstone Member|64856|4|Described|p92-93|Late Jurassic|Late Jurassic|Type section is in GSQ Roma 7. A well developed mudstone, sandstone, siltstone and coal unit in lower Westbourne Formation, Surat Basin. Upper Jurassic age implied.|| ||||29-NOV-17
14311|Norwood Mudstone Member|68117|5|Briefly described|p345|Late Jurassic|Late Jurassic|Surat Basin.||Westbourne Formation.||||
14311|Norwood Mudstone Member|69594|5|Briefly described|p537|Kimmeridgian|Kimmeridgian|Defined by Swarbrick et al. (1973). Low-energy back swamp and meandering stream channel deposits.||Westbourne Formation.|||Interbedded mudstone, lithic sandstone, siltstone and coal.|
14314|Nour Nour Granodiorite|24382|5|Briefly described|Map legend|Middle Triassic|Middle Triassic|||||||
14314|Nour Nour Granodiorite|41778|2|Defined|Table 1|Middle Triassic|Early Triassic|Described P373. Reserved as Nour Nour||||||
14314|Nour Nour Granodiorite|42054|6|Mentioned|p272|||||||||
14314|Nour Nour Granodiorite|43008|5|Briefly described|map legend|||||||||
14314|Nour Nour Granodiorite|63821|4|Described|p30|Middle Triassic|Early Triassic|Age: 238+/-3Ma (K-Ar biotite) and 235+/-3Ma (K-Ar hornblende). Intrudes Curtis Island Group and the Wolca Granite. Medium-grained hornblende-biotite granodiorite.||||||07-FEB-11
14314|Nour Nour Granodiorite|68679|5|Briefly described|p421-422|Middle Triassic|Middle Triassic|Gayndah-Gladstone belt.|238 Ma (K-Ar biotite: DA16-GSQ, 1983).||||Biotite-hornblende granodiorite, hornblende-biotite granodiorite, with two plagioclase generations.|
14376|Nullawurt Sandstone Member|23056|6|Mentioned|8 table 1B|||Geol province Surat Basin||||||
14376|Nullawurt Sandstone Member|23982|5|Briefly described|p58 Fig.18|||Of Bungil Formation. Geological Province: Surat Basin.||||||
14376|Nullawurt Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Of Bungil Formation. Geological Province: Surat Basin.||||||
14376|Nullawurt Sandstone Member|30021|6|Mentioned|p87|||||||||
14376|Nullawurt Sandstone Member|30022|6|Mentioned|p28|||||||||
14376|Nullawurt Sandstone Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14376|Nullawurt Sandstone Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
14376|Nullawurt Sandstone Member|30696|4|Described|Table 4|||Lower Cretaceous age||||||
14376|Nullawurt Sandstone Member|31116|4|Described|p42|||||||||
14376|Nullawurt Sandstone Member|31208|6|Mentioned|Table 1|||||||||
14376|Nullawurt Sandstone Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
14376|Nullawurt Sandstone Member|32314|6|Mentioned|Fig. 4|||||||||
14376|Nullawurt Sandstone Member|35648|6|Mentioned|p18|||||||||
14376|Nullawurt Sandstone Member|36552|6|Mentioned|p59|||||||||
14376|Nullawurt Sandstone Member|37995|6|Mentioned|p66|||||||||
14376|Nullawurt Sandstone Member|39211|5|Briefly described|p31|||||||||
14376|Nullawurt Sandstone Member|39212|4|Described|p39|||Excursion site. See also P18||||||
14376|Nullawurt Sandstone Member|39216|6|Mentioned|p55|||Fauna||||||
14376|Nullawurt Sandstone Member|40541|4|Described|p111|||||||||
14376|Nullawurt Sandstone Member|40666|4|Described|p358|||||||||
14376|Nullawurt Sandstone Member|41064|6|Mentioned|p60|||||||||
14376|Nullawurt Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
14376|Nullawurt Sandstone Member|42494|5|Briefly described|Table 1 P24|||||||||
14376|Nullawurt Sandstone Member|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
14376|Nullawurt Sandstone Member|44021|14|Not recorded|p232(Fig.1)|||||||||
14376|Nullawurt Sandstone Member|44377|2|Defined|p1,2,10,12-14,map||Neocomian|Freshwater. Member of Blythesdale Formation.||||||
14376|Nullawurt Sandstone Member|45103|6|Mentioned|p6|||||||||
14376|Nullawurt Sandstone Member|45110|4|Described|p111|||See also Table 18. Of Bungil Formation.||||||
14376|Nullawurt Sandstone Member|45132|6|Mentioned|Table 2|||||||||
14376|Nullawurt Sandstone Member|46791|6|Mentioned|Table 1|||||||||
14376|Nullawurt Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
14376|Nullawurt Sandstone Member|46984|6|Mentioned|Table 1|||||||||
14376|Nullawurt Sandstone Member|48919|6|Mentioned|Table 5|||||||||
14376|Nullawurt Sandstone Member|49010|6|Mentioned|Fig.4|||Surat Basin||||||
14376|Nullawurt Sandstone Member|49011|6|Mentioned|Fig.3|||Surat Basin||||||
14376|Nullawurt Sandstone Member|64856|5|Briefly described|p98,99|Early Cretaceous|Early Cretaceous|Of Day (1964). Originally included in Blythesdale Formation, now in Bungil Formation. Inferred to be of Lower Cretaceous age.|| ||||31-JAN-13
14376|Nullawurt Sandstone Member|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Bungil Formation.||Overlies Kingull Member. Is overlain by Minmi Member.||
14376|Nullawurt Sandstone Member|69594|5|Briefly described|p538|||Northern Surat Basin. Previously included by Day (1964) in his Blythesdale Formation. Marine and brackish water environment.||Bungil Formation.|||Quartzose fine sandstones with occasional shale partings and contains worm burrows, possible coprolites and freshwater bivalves.|
14376|Nullawurt Sandstone Member|70821|5|Briefly described|p80|||Surat Basin.||Bungil Formation.||Overlies Kingull Member. Is overlain by Minmi Member.||
14376|Nullawurt Sandstone Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||Bungil FZ.||Overlies Kingull Member. Is overlain by Minmi Member.||
14383|Numinbah Valley Formation|30687|4|Described|p65|||Tertiary age||||||
14383|Numinbah Valley Formation|33756|5|Briefly described|p263|||Refers McTaggart (1961)||||||
14383|Numinbah Valley Formation|39445|5|Briefly described|Table 14|||||||||
14383|Numinbah Valley Formation|44784|14|Not recorded|p12||Tertiary|Unit of Lamington Group.||||||
14383|Numinbah Valley Formation|44813|14|Not recorded|p80||Tertiary|||||||
14383|Numinbah Valley Formation|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|Overlain by the Lamington Group; overlies the Allandale Granite. Age: Thickness: 30m. In the Brisbane region.||||||
14383|Numinbah Valley Formation|69599|5|Briefly described|p595|Miocene|Miocene|Gold Coast hinterland and MacPherson Ranges. Up to 30m thick. Contains dicotyledonous leaves.||||Is overlain by Lamington Volcanics.|Shale and mudstone.|
14388|Nundah Granodiorite|23076|5|Briefly described|p723|Silurian|Silurian|||||||
14388|Nundah Granodiorite|23291|4|Described|p89 Fig. 3.8|Silurian|Ordovician|Parent: White Springs Supersuite. Age: 434Ma. Geological Province: Georgetown Region.||||||25-MAR-15
14388|Nundah Granodiorite|23422|5|Briefly described|Plate 7.3|Early Silurian|Late Ordovician|||||||
14388|Nundah Granodiorite|23423|5|Briefly described|p263|Early Silurian|Late Ordovician|Age: 434 +/- 10 Ma (SHRIMP)||||||
14388|Nundah Granodiorite|23430|5|Briefly described|p474|||Hodgkinson Province.||||||
14388|Nundah Granodiorite|23496|5|Briefly described|p47|Early Silurian|Late Ordovician|||||||
14388|Nundah Granodiorite|23500|5|Briefly described|Map legend|Early Silurian|Late Ordovician|Age: 434 +/- 10Ma, SHRIMP. White Springs Supersuite.||||||
14388|Nundah Granodiorite|23501|5|Briefly described|map legend|Early Silurian|Late Ordovician|White Springs (Blackman Gap) Supersuite.||||||
14388|Nundah Granodiorite|23510|5|Briefly described|Map Legend||Silurian|||||||
14388|Nundah Granodiorite|23513|5|Briefly described|Map legend||Silurian|Palaeozoic Intrusive No. 304. I-Type.||||||
14388|Nundah Granodiorite|23616|5|Briefly described|p65|||Previously mapped as part of Dargalong Metamorphics. Of Blackman Gap Supersuite.||||||
14388|Nundah Granodiorite|23624|6|Mentioned|p7|||||||||
14388|Nundah Granodiorite|23713|5|Briefly described|p76 Appendix 2, p15||Early Silurian|Intrudes Dargalong Metamorphics. Previously mapped as part of the Dargalong Metamorphics. Of Blackman Gap Supersuite. Dargalong Province.||||||
14388|Nundah Granodiorite|24485|5|Briefly described|p9 Tb.1|Early Silurian|Late Ordovician|Age: 434 +/- 9Ma (U-Pb SHRIMP zircon). Intrudes the Dargalong Metamorphics. Parent: White Springs Supersuite. Geological Province: Pama Province||||||
14388|Nundah Granodiorite|24486|5|Briefly described|Map legend|Early Silurian|Late Ordovician|Of the White Springs Supersuite.  Age: 434+/-9Ma (SHRIMP).  Geological Province: Pama Province.||||||
14388|Nundah Granodiorite|42765|5|Briefly described|p18, p21|||||||||
14388|Nundah Granodiorite|43060|5|Briefly described|p84|||of Blackman Gap Supersuite||||||
14388|Nundah Granodiorite|43083|4|Described|p115,p251.||Early Silurian|Of Blackmans Gap Supersuite. Previously mapped as Forsayth Granite by Best (1962; de Keyser and Wolff 1964).  Mainly medium- to coarse-grained leucocratic biotite-muscovite granodiorite. Detailed lithology included.||||||25-MAR-15
14388|Nundah Granodiorite|43087|2|Defined|p9|Early Silurian||||||||
14388|Nundah Granodiorite|43254|5|Briefly described|map legend||Early Silurian|of Blackman Gap Supersuite.||||||
14388|Nundah Granodiorite|43259|4|Described|Appendix 1,p37.||Silurian|Silurian, possibly Proterozoic in part.||||||25-MAR-15
14388|Nundah Granodiorite|43285|6|Mentioned|Map Legend|Early Silurian|Late Ordovician|of Blackman Gap Supersuite.||||||
14388|Nundah Granodiorite|43625|6|Mentioned|p10|Early Silurian|Late Ordovician|Age: 434+/-9 Ma||||||
14388|Nundah Granodiorite|60425|5|Briefly described|p22, p51 Tb. 3|Early Silurian|Late Ordovician|In Etheridge province. Age: 434+/-10Ma. Unconformably overlain by Pratt Volcanics.||||||07-FEB-11
14388|Nundah Granodiorite|62371|5|Briefly described|p472 Fig.3|Silurian|Silurian|Intrusive rocks.||||||
14388|Nundah Granodiorite|63140|6|Mentioned|p571 fig 2, p582, p583 Fig.13.|Early Silurian|Late Ordovician|West of the Hodgkinson Province.||||||03-APR-17
14388|Nundah Granodiorite|68337|5|Briefly described|Map legend|Early Silurian|Early Silurian|Pama Province. An un-named geophysical subdivision is mapped separately and described as "probably a variant of grey, foliated, medium-grained, biotite-muscovite and muscovite-biotite granodiorite".||Unit in White Springs Supersuite.|||Pale grey to white, variably foliated, fine- to medium-grained, uneven-grained to locally porphyritic muscovite-biotite granodiorite; minor pegmatite, aplite.|
14388|Nundah Granodiorite|69592|5|Briefly described|p282, p284 Fig.4.76, p297|Silurian|Silurian|Tate Batholith.|434 +/- 9 Ma (SHRIMP U-Pb zircon).|White Springs Supersuite.|||I-type.|
14388|Nundah Granodiorite|70207|4|Described|p5, p73-74, p77, p88, p90|Silurian|Silurian|Unit in Tate Batholith. Member of Pama Igneous Association. Cut by mineralised felsic dykes around the Mountain Maid Au deposit; and by a quartz-feldspar porphyry dyke (likely part of Ootann Supersuite) aged 317.7 +/- 2.7 Ma. The 434 Ma age is by Fanning (unpublished), reported by Bultitude et al. (1996).|434 +/- 9 Ma (U-Pb SHRIMP age).|White Springs Supersuite.||Cut by (probable) Ootann Supersuite.|I-type.|
14388|Nundah Granodiorite|70345|6|Mentioned|p3|Silurian|Silurian|Of the Pama Igneous Association.||||||
14388|Nundah Granodiorite|70673|6|Mentioned|p7|Silurian|Silurian|||||||
14441|Nymbool Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of Ootann Supersuite. Age: 318+/-43 Ma, Rb-Sr.||||||
14441|Nymbool Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 289. I-Type.||||||
14441|Nymbool Granite|23616|5|Briefly described|p99 Appendix 2||Carboniferous|||||||
14441|Nymbool Granite|29820|6|Mentioned|p450|||||||||
14441|Nymbool Granite|33963|6|Mentioned|Map legend|Permian|Permian|Prob. Permian||||||
14441|Nymbool Granite|39445|6|Mentioned|p90|||Blake(1972)||||||
14441|Nymbool Granite|42547|6|Mentioned|p75|||||||||
14441|Nymbool Granite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
14441|Nymbool Granite|45065|4|Described|Table 4|||||||||
14441|Nymbool Granite|45113|3|Fully described|p14|||Emphasis on petrography.||||||
14441|Nymbool Granite|46845|6|Mentioned|Table 1|||||||||
14441|Nymbool Granite|46879|6|Mentioned|Fig.1|||||||||
14441|Nymbool Granite|48976|4|Described|p47|||Isotopic data Table 12||||||
14441|Nymbool Granite|60425|4|Described|p276-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Nymbool Suite (Ootann Supersuite). Age: ~316Ma, 318+/-43Ma (Rb-Sr). I-type. Grey, fine- to med.gr.. Slightly porphyritic biotite granite; small biotite-rich inclusions common; minor aplite, aplitic biotite microgranite.||||||07-FEB-11
14449|O'Bil Bil Road Conglomerate|31586|6|Mentioned|p6|||Correlation of Visean coral horizons||||||
14449|O'Bil Bil Road Conglomerate|31587|6|Mentioned|p60|||Lithostrotion distribution||||||
14449|O'Bil Bil Road Conglomerate|32388|6|Mentioned|Fig.1|||||||||
14449|O'Bil Bil Road Conglomerate|32866|6|Mentioned|p22|||Fossil content||||||
14449|O'Bil Bil Road Conglomerate|42547|4|Described|p52|||||||||
14449|O'Bil Bil Road Conglomerate|44360|14|Not recorded|p13,30-32||Visean|Equivalent of Dakiel Formation.||||||
14449|O'Bil Bil Road Conglomerate|46803|6|Mentioned|p143|||||||||
14454|O'Hara Shale|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, chert, fine sandstone. Overlies: Selwyn Range Limestone, Devoncourt Limestone, Roaring Siltstone, Thorntonia Limestone.||||||27-AUG-04
14454|O'Hara Shale|22954|6|Mentioned|Fig3p9|Idamean|Mindyallan|||||||
14454|O'Hara Shale|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 50m.||||||
14454|O'Hara Shale|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
14454|O'Hara Shale|30778|6|Mentioned|Fig.5|||||||||
14454|O'Hara Shale|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14454|O'Hara Shale|31287|6|Mentioned|p430|||Refers Opik (1956)||||||
14454|O'Hara Shale|31396|6|Mentioned|Fig.3|||||||||
14454|O'Hara Shale|31572|4|Described|Fig.|||U.Cambrian||||||
14454|O'Hara Shale|32952|6|Mentioned|p1188|||See also p1189. M.-U. Camb.||||||30-JAN-07
14454|O'Hara Shale|33111|4|Described|p41|||||||||
14454|O'Hara Shale|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
14454|O'Hara Shale|34287|6|Mentioned|Fig.3|||||||||
14454|O'Hara Shale|35054|6|Mentioned|Table 23|||||||||
14454|O'Hara Shale|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
14454|O'Hara Shale|35139|4|Described|Table.2|||||||||
14454|O'Hara Shale|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14454|O'Hara Shale|37572|4|Described|p160|||See also Fig.8||||||
14454|O'Hara Shale|37816|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
14454|O'Hara Shale|38350|6|Mentioned|p22|||||||||
14454|O'Hara Shale|38444|6|Mentioned|p106|||||||||
14454|O'Hara Shale|38446|6|Mentioned|Table 23|||||||||
14454|O'Hara Shale|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14454|O'Hara Shale|39029|5|Briefly described|Map legend|Cambrian|Cambrian|Overlies Roaring Siltstone unconformably; underlies Pomegranate Limestone unconformably.||||||25-AUG-04
14454|O'Hara Shale|39445|5|Briefly described|Table 4|||See also p62.||||||30-JAN-07
14454|O'Hara Shale|39690|6|Mentioned|p92|||||||||
14454|O'Hara Shale|41810|6|Mentioned|p112|||||||||
14454|O'Hara Shale|42139|6|Mentioned|Fig.19 P74|||||||||
14454|O'Hara Shale|43883|14|Not recorded|p18 Fig.4-3|||||||||
14454|O'Hara Shale|44091|14|Not recorded|p17,Tb.1|Idamean|Mindyallan|Partial equivalent of Pomegranate Limestone.||||||
14454|O'Hara Shale|44205|2|Defined|p5,9-19,22-30,39-40,||Late Cambrian|p134,154,179-185. Overlies Selwyn Range Ls, Devoncourt Ls and Pomegranate Ls. (Dresbachian = lower Upper Cambrian)||||||
14454|O'Hara Shale|44211|2|Defined|p5,9,10,14-5,19,22-8||Late Cambrian|p30,32,39-40,134,154,179-80,184-5. Contemporaneous with Pomegranate Limestone. (Dresbachian {lower Upper Cambrian})||||||
14454|O'Hara Shale|44275|14|Not recorded|Map Legend|||||||||
14454|O'Hara Shale|44276|2|Defined|p6,7,18,20,22,Tb.2,|||map.||||||
14454|O'Hara Shale|44277|14|Not recorded|Map Legend||Late Cambrian|||||||
14454|O'Hara Shale|44291|14|Not recorded|p7|||||||||
14454|O'Hara Shale|44361|14|Not recorded|Map Legend||Late Cambrian|||||||
14454|O'Hara Shale|44362|4|Described|p9,Tb.1||Late Cambrian|||||||
14454|O'Hara Shale|44543|14|Not recorded|p32,36|||See also Lexicon.||||||
14454|O'Hara Shale|44666|14|Not recorded|p481||Late Cambrian|||||||
14454|O'Hara Shale|44920|14|Not recorded|Map Legend, Sheet 4||Late Cambrian|||||||
14454|O'Hara Shale|45002|14|Not recorded|p10-118|||Early/Late Cambrian fossils.||||||30-JAN-07
14454|O'Hara Shale|45012|14|Not recorded|p92-99,104-7,131-44|||p152-67,171-88,203-6,219-228,250-56,316-390. Fauna in 'lower chert bed'.||||||
14454|O'Hara Shale|45051|6|Mentioned|p4|||Seed also p9. Cambrian age.||||||30-JAN-07
14454|O'Hara Shale|45052|3|Fully described|p113|||U.Camb. See also p33.||||||30-JAN-07
14454|O'Hara Shale|45079|4|Described|p36|||Cambrian age||||||
14454|O'Hara Shale|45130|6|Mentioned|p3|||||||||
14454|O'Hara Shale|45166|5|Briefly described|Table 15|||||||||
14454|O'Hara Shale|50100|5|Briefly described|p22|Late Cambrian|Late Cambrian|Laminated to thin-bedded and commonly iron-stained, covered by duricrust or lateritic gravel. Conformably overlain by and interfingered with Pomegranate Limestone; conformably overlies the Devoncourt Limestone..||||||
14454|O'Hara Shale|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone; minor chert, sandstone.||||||
14454|O'Hara Shale|64068|4|Described|p70, p64, 67, 69|Late Cambrian|Late Cambrian|Diverse trilobite, brachiopod fauna. Correlated with Arrinthrunga Formation, Georgina Limestone. Maximum thickness 100m.||Of Narpa Group.||Conformably overlies Devoncourt and Selwyn Range Limestones (also laterally interdigitates with Selwyn). Conformably overlain by, and interdigitates with, Pomegranate Limestone.|Ferruginised micaceous shale and siltstone; sandstone and chert interbeds.|21-MAR-16
14454|O'Hara Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p83|Late Cambrian|Late Cambrian|Burke River Structural Belt, Georgina Basin.||Of Narpa Group.||Overlies Selwyn Range Limestone. Is overlain by Pomegranate Limestone.|Siltstone; minor chert, sandstone; lateritic rubble capping|
14454|O'Hara Shale|67870|6|Mentioned|p39, p43-46|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Part of a ~600m thick package with high amplitude discontinuous seismic reflections.||||||
14454|O'Hara Shale|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Siltstone; minor chert and sandstone; lateritic rubble capping|
14454|O'Hara Shale|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
14454|O'Hara Shale|69573|6|Mentioned|p659, 661, 669|||Georgina Basin.||||||
14454|O'Hara Shale|69591|5|Briefly described|p87, p93-94, p96|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. [Relationship accounts with Pomegranate Limestone are contradictory.]||Narpa Group.||Overlies Selwyn Range Limestone and, gradationally, Pomegranate Limestone (and interfingers with it).||
14454|O'Hara Shale|72321|6|Mentioned|Fig 2|Pabian|Guzhangian|Burke River Structural Belt, Georgina Basin.  Australian stages: Mindyallan to Idamean.||of Narpa Group.||||
14454|O'Hara Shale|72516|6|Mentioned|p93-94|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arrinthrunga Formation and the Eurowie Sandstone Member.||08-JUN-21
14454|O'Hara Shale|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Partially overlies Selwyn Limestone.|Siltstone; minor chert and sandstone; lateritic rubble capping.|
14454|O'Hara Shale|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Overlies Selwyn Range Limestone.|Siltstone; minor chert and sandstone; lateritic rubble capping.|
14458|Oak River Granodiorite|9541|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Grey foliated medium-grained biotite granodiorite.||||||
14458|Oak River Granodiorite|22611|6|Mentioned|P189||Silurian|||||||
14458|Oak River Granodiorite|22669|6|Mentioned|P251|Devonian|Silurian|||||||
14458|Oak River Granodiorite|23032|4|Described|p38||Early Devonian|Rb/Sr Ages: 388 to 400 Ma.||||||
14458|Oak River Granodiorite|23220|5|Briefly described|Fig.2, p14|Early Devonian|Late Silurian|||||||
14458|Oak River Granodiorite|23291|4|Described|p89 Fig. 3.8|||Parent: White Springs Supersuite. Geological Province: Georgetown Region.||||||28-MAY-15
14458|Oak River Granodiorite|23430|5|Briefly described|p486|||||||||
14458|Oak River Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 28. I-Type.||||||
14458|Oak River Granodiorite|23619|4|Described|p41 Table 2|Early Devonian|Silurian|Also see p7. Copperfield Batholith Georgetown Province.||||||
14458|Oak River Granodiorite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14458|Oak River Granodiorite|33907|6|Mentioned|p4|||||||||
14458|Oak River Granodiorite|33909|2|Defined|p230|Proterozoic|Proterozoic|||||||
14458|Oak River Granodiorite|35920|6|Mentioned|p21|||Defined by Withnall & others 1976.||||||
14458|Oak River Granodiorite|37570|4|Described|p120|||||||||
14458|Oak River Granodiorite|37571|6|Mentioned|p133|||||||||
14458|Oak River Granodiorite|37576|5|Briefly described|p8|||||||||
14458|Oak River Granodiorite|39445|5|Briefly described|Table 2|||See also P45||||||
14458|Oak River Granodiorite|39687|6|Mentioned|p3|||See also P25||||||
14458|Oak River Granodiorite|39689|6|Mentioned|Fig.2|||||||||
14458|Oak River Granodiorite|39917|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian-Early Devonian||||||
14458|Oak River Granodiorite|39981|1|Redefined|p104|Devonian|Silurian|Silurian-Devonian age||||||
14458|Oak River Granodiorite|40798|5|Briefly described|p237|||||||||
14458|Oak River Granodiorite|41272|5|Briefly described|p27|||See also M 1of1 H05||||||
14458|Oak River Granodiorite|41574|6|Mentioned|p405|||||||||
14458|Oak River Granodiorite|41680|3|Fully described|p123|||||||||
14458|Oak River Granodiorite|41807|5|Briefly described|p62|||||||||
14458|Oak River Granodiorite|43103|6|Mentioned|p16|||||||||
14458|Oak River Granodiorite|43113|4|Described|Table 2 p26|Early Devonian|Silurian|Minimum age of 400 Ma (Bain & others,in prep)||||||
14458|Oak River Granodiorite|43253|5|Briefly described|map legend|Early Devonian|Silurian|||||||
14458|Oak River Granodiorite|43259|4|Described|Appendix 1,p17.|Early Devonian|Late Silurian|||||||
14458|Oak River Granodiorite|43286|5|Briefly described|Map Legend|Early Devonian|Silurian|||||||
14458|Oak River Granodiorite|43480|6|Mentioned|58|||||||||
14458|Oak River Granodiorite|43664|6|Mentioned|p82,94|||||||||
14458|Oak River Granodiorite|43716|6|Mentioned|p82|||||||||
14458|Oak River Granodiorite|50199|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
14458|Oak River Granodiorite|50201|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
14458|Oak River Granodiorite|50211|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Grey, commonly foliated, equigranular hornblende-biotite tonalite and biotite tonalite or granodiroite.||||||14-MAY-04
14458|Oak River Granodiorite|67113|6|Mentioned|p408 Fig.2|||Georgetown Inlier, Australian Craton.|~420 Ma.|||||
14458|Oak River Granodiorite|68346|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Unit in Copperfield Batholith. Moderately magnetic.|||||Grey, commonly foliated, equigranular to porphyritic, hornblende-biotite tonalite and biotite tonalite or granodiorite; some areas containing abundant xenoliths and roof-pendants of metamorphic rocks.|
14458|Oak River Granodiorite|68353|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Copperfield Batholith, Pama Province.|||||Grey, locally foliated, porphyritic biotite granodiorite; grey, commonly foliated, equigranular hornblende-biotite tonalite and biotite tonalite or granodiorite.|
14458|Oak River Granodiorite|68357|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Pama Province.|||||Grey, commonly foliated, equigranular hornblende-biotite tonalite and biotite tonalite or granodiorite.|
14458|Oak River Granodiorite|68576|6|Mentioned|Q_11: p30-31|||Einasleigh area. A main component of the Copperfield Batholith. Part of the Pama Igneous Association. Poor outcrop.||||||
14458|Oak River Granodiorite|69592|5|Briefly described|p282-285|Silurian|Silurian|Champion (1991) recognised the composite character of this unit. The porphyritic biotite granodiorite part of this unit is assigned to the White Springs Supersuite, while the equigranular tonalite part to the Dido Supersuite.|417.7 +/- 2.2 Ma (SHRIMP U-Pb zircon).|White Springs Supersuite.|||I-type.|
14470|Oakleigh Siltstone Member|13516|5|Briefly described|p147, fig 5|Late Carboniferous|Late Carboniferous|From Galilee Basin||Of Jericho Formation||||
14470|Oakleigh Siltstone Member|30915|6|Mentioned|p100|||||||||
14470|Oakleigh Siltstone Member|31120|6|Mentioned|p149|||||||||
14470|Oakleigh Siltstone Member|31122|2|Defined|p349|Early Permian|Late Carboniferous|Probably Late Carboniferous to Early Permian.||||||
14470|Oakleigh Siltstone Member|31258|6|Mentioned|Table 1|||||||||
14470|Oakleigh Siltstone Member|31860|6|Mentioned|p280|||||||||
14470|Oakleigh Siltstone Member|33372|6|Mentioned|p16|||||||||
14470|Oakleigh Siltstone Member|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
14470|Oakleigh Siltstone Member|36243|6|Mentioned|Table 5A|||||||||
14470|Oakleigh Siltstone Member|36921|6|Mentioned|p174|||See also Table 1.||||||
14470|Oakleigh Siltstone Member|39478|6|Mentioned|Table 1|||||||||
14470|Oakleigh Siltstone Member|39847|6|Mentioned|p34|||||||||
14470|Oakleigh Siltstone Member|39943|6|Mentioned|Table 7A|||||||||
14470|Oakleigh Siltstone Member|41198|6|Mentioned|Table 1|||||||||
14470|Oakleigh Siltstone Member|42547|5|Briefly described|p80|||||||||
14470|Oakleigh Siltstone Member|43105|6|Mentioned|p13|||of Jericho Formation?||||||
14470|Oakleigh Siltstone Member|43812|6|Mentioned|Fig.3,p145|||||||||
14470|Oakleigh Siltstone Member|46849|6|Mentioned|Fig. 7|||||||||
14470|Oakleigh Siltstone Member|65489|6|Mentioned|p144 Fig.53|Permian|Permian|Koburra Trough, Galilee Basin.||||||
14470|Oakleigh Siltstone Member|66188|6|Mentioned|435, 439, Fig 3,17|Early Permian|Late Carboniferous|Included in the Jericho Formation for the purposes of this study. Sequence boundary at base.||||||
14470|Oakleigh Siltstone Member|67402|6|Mentioned|p125 tbl GLL1, p128 fig GLL8, p132|Sakmarian|Asselian|Galilee Basin. Deposited in a lacustrine environment.||Jericho Formation|||Mudstone and siltstone.|
14470|Oakleigh Siltstone Member|68279|6|Mentioned|p4|Moscovian|Moscovian|Galilee Basin.||Unit in Jericho Formation.||||
14470|Oakleigh Siltstone Member|68731|6|Mentioned|p198, p201 Fig 3.110|Pennnsylvanian|Pennnsylvanian|||Of the Jericho Formation.||||
14470|Oakleigh Siltstone Member|71265|5|Briefly described|p589|Moscovian|Moscovian|Galilee Basin.||Jericho Formation.||||
14470|Oakleigh Siltstone Member|71701|5|Briefly described|p155-p156|Moscovian|Moscovian|Central Western Area, Eastern Area, Galilee Basin.||Jericho Formation||||
14470|Oakleigh Siltstone Member|71710|4|Described|p370 , p374-377, p381, p384, p385, p386|Late Carboniferous|Late Carboniferous|Geological province: Galilee Basin. More arenaceous in Koburra-1 vs. Lake Galilee-1. Depositional environment, well log character and sequence stratigraphy described. Fluvial channel and lacustrine facies.||Probably of Jericho Formation. Forms part of sequence 2, this paper.||Fine-grained, coarsening upwards to become the upper Jericho Formation. Underlain by lower Jericho Formation.|Interbedded siltstone (calcareous in places), mudstone and shale, becoming more arenaceous to the north. Sand contains red lithic grains of a tuffaceous origin.|
14470|Oakleigh Siltstone Member|72088|4|Described|p8, p17, p91|Moscovian|Moscovian|Southern Galilee Basin in the Koburra Trough. Tuff bands in the lacustrine facies indicate local volcanism.||Jericho Formation|||Banded and varved siltstone, mudstone and shale.|
14470|Oakleigh Siltstone Member|73163|5|Briefly described|p467|Asselian|Asselian|Galilee Basin. Found in the upper part of the Jericho Formation.||Upper part of Jericho Formation.|||Series of interbedded siltstones, mudstones, and shales.|
14470|Oakleigh Siltstone Member|73472|6|Mentioned|p115|Moscovian|Moscovian|Galilee Basin.||Jericho Formation, Joe Joe Group||||
14476|Oakvale Conglomerate|35937|6|Mentioned|Fig.4|||||||||
14476|Oakvale Conglomerate|37110|5|Briefly described|p288|||||||||
14590|One Tree Granite|24197|5|Briefly described|p21, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Age: 1860Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
14590|One Tree Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14590|One Tree Granite|37862|4|Described|p584|||||||||
14590|One Tree Granite|38310|6|Mentioned|p237|||||||||
14590|One Tree Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14590|One Tree Granite|38900|6|Mentioned|p55|||||||||
14590|One Tree Granite|39445|5|Briefly described|Table 2|||||||||
14590|One Tree Granite|40840|6|Mentioned|Map legend|||||||||
14590|One Tree Granite|45161|4|Described|p27|||||||||
14590|One Tree Granite|45166|6|Mentioned|p10|||||||||
14590|One Tree Granite|49009|2|Defined|p31|Paleoproterozoic|Paleoproterozoic|Previously mapped as Kalkadoon Granite (Carter and Opik,1963).||||||07-NOV-08
14590|One Tree Granite|49041|5|Briefly described|Table 2|||||||||
14590|One Tree Granite|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Kalkadoon Batholith.  Overlain unconformably by Leichhardt Volcanics.||||||
14590|One Tree Granite|50536|5|Briefly described|p1.4 Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
14590|One Tree Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Pale to dark biotite granite, commonly porphyritic and foliated.||||||
14590|One Tree Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map., p14|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block.||Kalkadoon Suite or Supersuite|||Medium to coarse biotite granite, locally porphyritic, minor microgranite, aplite, pegmatite. Massive to strongly foliated.|
14590|One Tree Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province.||Kalkadoon Suite.|||Medium to coarse biotite granite, locally porphyritic, minor microgranite, aplite, pegmatite; massive to strongly foliated.|
14590|One Tree Granite|73137|6|Mentioned|p1, p90, p93|Orosirian|Orosirian|Similar in age to Plum Mountain Gneiss and a sample tentatively assigned[?] to the Birds Well Granite [ca. 1863 Ma].|1860 Ma|||||
14590|One Tree Granite|73413|6|Mentioned|p5-6, p9-10, p21|Orosirian|Orosirian|[Also written as One Tree granite]. New U-Pb zircon age of 1857 +/- 5 Ma reported herein. A remnant was identified immediately west of Tick Hill[?].|1857 +/- 5 Ma|Kalkadoon Supersuite|||Includes granitic gneiss.|
14590|One Tree Granite|73553|6|Mentioned|p6, p8 Fig.1.2.3, p253-254|||Kalkadoon-Leichhardt Domain. Interpreted to intrude Plum Mountain Gneiss.||Kalkadoon Suite||||
14620|Ootann Supersuite|23076|5|Briefly described|p724|Stephanian|Westphalian|306-299 M yr||||||
14620|Ootann Supersuite|23291|3|Fully described|p45, p96 Tb 3.11, p101 Tb. 3.13|Permian|Carboniferous|Geological Province: Georgetown Region.||||||02-JUN-09
14620|Ootann Supersuite|23420|4|Described|p 147 table 4.6|Early Permian|Late Carboniferous|Intrudes Chelmsford Gneiss, Yambo Metamorphic Group. In the Cape York Penninsula Batholith.||||||24-JUN-15
14620|Ootann Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Late Carboniferous|||||||
14620|Ootann Supersuite|23423|4|Described|p315 Table 7.4|Early Permian|Late Carboniferous|I-type. Age: ~316 Ma to ~290 Ma (Rb-Sr). Intrudes Hodgkinson Province. Also see p243. Kennedy Igneous Province.||||||
14620|Ootann Supersuite|23500|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
14620|Ootann Supersuite|23501|6|Mentioned|map legend|Late Carboniferous|Late Carboniferous|||||||
14620|Ootann Supersuite|23502|5|Briefly described|Map Legend||Late Carboniferous|||||||
14620|Ootann Supersuite|23503|5|Briefly described|Map Legend|||||||||
14620|Ootann Supersuite|23506|5|Briefly described|Map Legend||Late Carboniferous|||||||
14620|Ootann Supersuite|23549|5|Briefly described|p527|||Interdigitates with the O'Briens Creek Supersuite.  See also p516 Fig. 1.||||||05-APR-05
14620|Ootann Supersuite|23616|4|Described|Table 3 p50, p71-75|Permian|Carboniferous|I-type Supersuite. Emplaced in three main episodes, about 10-20 Ma apart. Dargalong Province. Also in Hodgkinson Province.||||||
14620|Ootann Supersuite|23617|5|Briefly described|p55|||I-type granite.||||||
14620|Ootann Supersuite|23624|3|Fully described|p9|Carboniferous|Carboniferous|Formerly the Ootann Suite.||||||08-JUL-15
14620|Ootann Supersuite|23713|5|Briefly described|p28||Carboniferous|Age: 310 Ma to 300 Ma.||||||
14620|Ootann Supersuite|24485|5|Briefly described|p45|Late Carboniferous|Late Carboniferous|||||||
14620|Ootann Supersuite|24486|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|||||||
14620|Ootann Supersuite|24512|5|Briefly described|p7|Carboniferous|Carboniferous|In the Kidston, Red Dome area.||||||
14620|Ootann Supersuite|42681|6|Mentioned|p20|||||||||
14620|Ootann Supersuite|43060|4|Described|p97|||||||||
14620|Ootann Supersuite|43083|4|Described|p122-p124|||Emplacement age of 300 Ma. Ranges from grey hornblende-biotite granodiorite to pale pink leucoadamellite and quartz monzonite.||||||17-JUN-09
14620|Ootann Supersuite|43087|6|Mentioned|p18|||||||||
14620|Ootann Supersuite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Includes Ootann Suite and Ootann Granite.||||||15-JUN-06
14620|Ootann Supersuite|43254|5|Briefly described|map legend|Early Permian|Late Carboniferous|Age Late Carboniferous to Early Permian?||||||
14620|Ootann Supersuite|43285|5|Briefly described|Map Legend|||age Late Carboniferous-Early Permian?||||||
14620|Ootann Supersuite|43625|6|Mentioned|p36|||||||||
14620|Ootann Supersuite|44246|6|Mentioned|Map Legend|Early Permian|Early Carboniferous|(Middle Carboniferous - Early Permian)||||||
14620|Ootann Supersuite|44926|5|Briefly described|Map Legend||Late Carboniferous|||||||
14620|Ootann Supersuite|60425|3|Fully described|p60 Tb. 4, p73-74, p276-7 Appdx. |Early Permian|Late Carboniferous|Includes California Creek, Nymbool, Ootann Suites+ ~50 formal/informal subunits. I-type. Age:~316Ma-290Ma (Rb-Sr). Intruded Hodgkinson Prov.+ Featherbed Volc.Gp (older units), Almaden Supersuite; cut by Lags Sup'ste microgranite.V.detailed lith. included||||||07-FEB-11
14620|Ootann Supersuite|61784|5|Briefly described|p297|||Of Mount Surprise-Herberton Group.||||||25-JAN-06
14620|Ootann Supersuite|62371|5|Briefly described|p472 Fig.3|Carboniferous|Carboniferous|I-type granite.||||||
14620|Ootann Supersuite|62523|5|Briefly described|Map legend at p3-4|Early Permian|Late Carboniferous|Includes the Ootann Suite.||||||07-FEB-11
14620|Ootann Supersuite|63140|6|Mentioned|p572 fig 3|Carboniferous|Carboniferous||||||I-type.|
14620|Ootann Supersuite|63154|5|Briefly described|p281 Fig. 3, p285 Fig. 5|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province and Georgetown Inlier. Granites are I-type.||||||11-APR-07
14620|Ootann Supersuite|68330|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes the Baldick, Barwidgi, Brookers Waterhole, Soda Spring, Bird Spring, Whistler, Junevale, Sheba, Gelaro, Crane Creek, Rices Creek and Frog Hollow Granites; Minnemore and Mount Pudding Basin Granodiorites; and Martin Creek Microgranite.|||Includes (inter alia) the Saucebottle, Mount Cardwell, Mountain Camp, California, Reddicliffe, Rudd, Rattler, Swamp Creek, Sandy Tate, Flat Rock, Mulindie, Teddys Creek and Koogangoona Granites|||17-DEC-13
14620|Ootann Supersuite|68331|5|Briefly described|Map legend.|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes the Barwidgi, Brookers Waterhole, Soda Spring, Bird Spring, Whistler, Junevale, Sheba, Gelaro, Crane Creek, Rices Creek and Frog Hollow Granites; Minnemore and Mount Pudding Basin Granodiorites; and Martin Creek Microgranite.|||Includes (inter alia) the Saucebottle, Mount Cardwell, Mountain Camp, California, Reddicliffe, Opah, Rudd, Rattler, Swamp Creek, Sandy Tate, Flat Rock, Mulindie, Teddys Creek and Koogangoona Granites|||
14620|Ootann Supersuite|68337|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Kennedy Province. Also includes Retchford, Borneo, Halpin, Torpys, Jacks, Stirlington, Bamford, Coonbeta, Election, Bungabilly, James Creek, Convict, Pinchgut, Bulluburrah, Worcester and Walkunder Granites; Martin Creek Microgranite; Sunnymount Granodiorite; and Cottell Rhyolite.|||Includes, inter alia, Batcha, Saucebottle, Sheba, Kitchener, Reddicliffe, "P", Indicator, Ootann, David, Lucy, Burke, Bismarck, Calcifer, Quaker, Koorboora, Billycan, Carrs and Petford Granites.|||
14620|Ootann Supersuite|68405|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Kennedy Province|||Arden Granite, Amber Granite, Frenchy Creek Granite, Rices Creek Granite, Gelaro Granite, Ixe Microgranodiorite, Junevale Granite, Mount Garling Granite, Whistler Granite, Saucebottle Granite.|Younger than White Springs Supersuite rocks.||
14620|Ootann Supersuite|68553|6|Mentioned|Map legend|Early Permian|Carboniferous|This unit (in part), as well as the Claret Creek, Glenmore, Ingham (in part), O'Briens Creek (in part), Almaden and Oweenee Supersuites; the Emerald Creek Suite; the Bedarra Granite Complex; the Montgomery Range Igneous Complex; and various ungrouped Carboniferous plutonic units, are all mapped under the same symbol, Cgk. It is also mapped (in part), as CPgk, with the Badu Suite and parts of the Almaden, Leichhardt, O'Briens Creek and Ingham Supersuites and various ungrouped Carboniferous-Early Permian plutonic units.||||||
14620|Ootann Supersuite|68576|5|Briefly described|Q_11: p12-14, p16|||Petford area. One of three voluminous Carboniferous to Permian Supersuites in the local area. Representative of the Kennedy Igneous Association.|||David Granite.|||
14620|Ootann Supersuite|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Palmer-Barron Subprovince, Hodgkinson Province.|308.6 +/- 3.9 Ma||||I-type granitoids.|
14620|Ootann Supersuite|69593|3|Fully described|p484-486,p488-489,p502-504,p506 Fig.6.26|Permian|Late Carboniferous|See also p508-510. Herberton and/or Tate Subprovinces, Kennedy Igneous Association. Extensive outcrops (over ~5,000 km2) on both sides of Palmerville Fault, near Chillagoe. Over 70 identified plutons within numerous Suites. Has similarities with Glenmore and Oweenee Supersuites. Associated with W-Mo-Bi and/or Au deposits. Geochemistry detailed. Other ages given and discussed; generally ~330-290 Ma.|304.7 +/- 1.6 Ma.||Ootann Suite; California Creek, Emerson Gap, Froghollow, Ootann, Rudd, Borneo Granites; Ixe Monzogranite.|Intrudes Almaden Supersuite.|Porphyritic to equigranular hornblende-biotite granodiorite to biotite granite and leucogranite; allanite is a conspicuous accessory phase in many of the granitoids; magnetite- and/or ilmenite-bearing. I-type.|
14620|Ootann Supersuite|70207|5|Briefly described|p5, p90|||Commonly associated with W-Mo-Bi-Au mineralisation ~45km W of Chillagoe. A porphyry dyke, likely part of the Supersuite, is dated 317.7 +/- 2.7 Ma.||||Probably cuts Nundah Granodiorite.|I-type granitoids.|
14620|Ootann Supersuite|71592|5|Briefly described|Appendix A.||||318+/-2.7 Ma (SHRIMP U-Pb zircon).||||Porphyry.|
14635|Orallo Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499, p501|Early Cretaceous|Tithonian|N Surat Basin. Originally named the Fossil Wood Stage (Reeves, 1947). Also known for a while as Orallo Coal Measures (Jensen, 1926), but the coal was uneconomic. 150-200m thick.|||||Cross-bedded labile to sub-labile sandstone with minor conglomerate, carbonaceous siltstone, mudstone, bentonite and thin banded seams of coal; fossil wood is ubiquitous.|
14635|Orallo Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
14635|Orallo Formation|22757|5|Briefly described|Table6,p12|Late Jurassic|Late Jurassic|245 m. Surat Basin||||||
14635|Orallo Formation|22857|4|Described|p296-7 Tb.22.1, p546 App.1 Tb.A1.12|Berriasian|Tithonian|Of the Blythesdale Group. Fine to medium-grained clayey arenite interbedded with carbonaceous siltstone and shales. Max. thickness: 230m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
14635|Orallo Formation|22865|4|Described|p314,Table22.1p296-7|Berriasian|Tithonian|||||||
14635|Orallo Formation|23050|4|Described|p23 Table 4|Late Jurassic|Late Jurassic|Of Surat Basin. Palynology indicates a J6 Jurassic age.||||||08-APR-13
14635|Orallo Formation|23051|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|Of Surat Basin.||||||13-MAR-09
14635|Orallo Formation|23053|6|Mentioned|Fig10p17,26|Tithonian|Kimmeridgian|||||||
14635|Orallo Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
14635|Orallo Formation|23740|5|Briefly described|p1221|Jurassic|Jurassic|Geological Province: Durat Basin||||||
14635|Orallo Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Late Jurassic|Geological Province: Surat Basin.  Maximum thickness: 230m.||||||
14635|Orallo Formation|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
14635|Orallo Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|24160|6|Mentioned|p18|Cretaceous|Cretaceous|Miles district, 350 km W of Brisbane. Major source of bentonite.||||||
14635|Orallo Formation|29387|6|Mentioned|Table 5|||||||||
14635|Orallo Formation|29393|6|Mentioned|Table 4|||||||||
14635|Orallo Formation|29591|6|Mentioned|Table 15|||||||||
14635|Orallo Formation|29721|6|Mentioned|Table 246|||||||||
14635|Orallo Formation|29870|4|Described|p15|||||||||
14635|Orallo Formation|30021|6|Mentioned|p90|||||||||
14635|Orallo Formation|30022|6|Mentioned|p32|||||||||
14635|Orallo Formation|30024|6|Mentioned|p332|||||||||
14635|Orallo Formation|30102|6|Mentioned|p26|||||||||
14635|Orallo Formation|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30694|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30695|4|Described|Table 4|||Upper Jurassic age||||||
14635|Orallo Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic age||||||
14635|Orallo Formation|30697|6|Mentioned|p34|||Minor aquifer present||||||
14635|Orallo Formation|30698|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper JurassicM - U||||||
14635|Orallo Formation|30701|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30702|4|Described|p49|||See also P51, Fig.1 & 2, Table 1.||||||
14635|Orallo Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
14635|Orallo Formation|31086|6|Mentioned|p37|||Faunas||||||
14635|Orallo Formation|31097|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|31098|5|Briefly described|Table 1|||||||||
14635|Orallo Formation|31116|4|Described|p38|||See also P39-40||||||
14635|Orallo Formation|31208|6|Mentioned|Fig. 5|||||||||
14635|Orallo Formation|31244|6|Mentioned|p8|||||||||
14635|Orallo Formation|31369|6|Mentioned|Table 4|||Jurassic||||||
14635|Orallo Formation|31376|6|Mentioned|p4|||||||||
14635|Orallo Formation|32136|6|Mentioned|p9|||Miospores||||||
14635|Orallo Formation|32138|6|Mentioned|p398|||||||||
14635|Orallo Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
14635|Orallo Formation|32276|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|32797|4|Described|Table 4|||||||||
14635|Orallo Formation|33070|4|Described|Table 2|||U.Jur.||||||
14635|Orallo Formation|33071|6|Mentioned|p6|||L.Cret.||||||
14635|Orallo Formation|33075|6|Mentioned|p451|||||||||
14635|Orallo Formation|33080|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33090|4|Described|Table 4|||U.Jur.||||||
14635|Orallo Formation|33091|5|Briefly described|p10|||Stratigraphy||||||
14635|Orallo Formation|33094|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33367|5|Briefly described|Table 1|||||||||
14635|Orallo Formation|33368|6|Mentioned|p21|||U.Jur.Oil shale.Refers Jensen (1926).||||||
14635|Orallo Formation|33451|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33672|6|Mentioned|p44|||||||||
14635|Orallo Formation|34134|6|Mentioned|Cor.Chart|||Upper Jurassic.||||||
14635|Orallo Formation|34212|6|Mentioned|p2|||Jurassic.||||||
14635|Orallo Formation|34254|6|Mentioned|p489|||L. Jurassic||||||
14635|Orallo Formation|34408|6|Mentioned|p185|||On Table||||||
14635|Orallo Formation|34543|6|Mentioned|p98|||||||||
14635|Orallo Formation|34613|4|Described|Table 4|||||||||
14635|Orallo Formation|35016|6|Mentioned|p41|||||||||
14635|Orallo Formation|35793|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|35937|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|36243|6|Mentioned|Table 7A|||||||||
14635|Orallo Formation|36570|2|Defined|p45|Jurassic|Jurassic|Also mentioned Fig.9, Table 1, P46, P60.||||||
14635|Orallo Formation|36939|6|Mentioned|p214|||||||||
14635|Orallo Formation|37117|5|Briefly described|p313|||||||||
14635|Orallo Formation|37856|6|Mentioned|Table I|||||||||
14635|Orallo Formation|37995|4|Described|p65|||||||||
14635|Orallo Formation|38199|6|Mentioned|p428|||||||||
14635|Orallo Formation|39212|5|Briefly described|p17|||See also P38||||||
14635|Orallo Formation|39315|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|39445|5|Briefly described|Table 10|||||||||
14635|Orallo Formation|39494|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|39666|6|Mentioned|p112, 111|||||||||
14635|Orallo Formation|39708|6|Mentioned|p477|||||||||
14635|Orallo Formation|39942|6|Mentioned|p465|||||||||
14635|Orallo Formation|39943|6|Mentioned|Table 9A|||||||||
14635|Orallo Formation|39998|5|Briefly described|p193|||||||||
14635|Orallo Formation|40030|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|40245|6|Mentioned|Table 2|||||||||
14635|Orallo Formation|40249|6|Mentioned|p38|||||||||
14635|Orallo Formation|40250|6|Mentioned|Fig.1|||||||||
14635|Orallo Formation|40540|6|Mentioned|p155|||||||||
14635|Orallo Formation|40541|3|Fully described|p110|||||||||
14635|Orallo Formation|40544|6|Mentioned|Fig.6|||||||||
14635|Orallo Formation|40666|4|Described|p357|||||||||
14635|Orallo Formation|40675|6|Mentioned|Table 9A|||||||||
14635|Orallo Formation|40687|6|Mentioned|p417|||Mention P421||||||
14635|Orallo Formation|40767|4|Described|p13|||||||||
14635|Orallo Formation|41060|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|41064|6|Mentioned|p60|||||||||
14635|Orallo Formation|41187|6|Mentioned|Fig.2|||||||||
14635|Orallo Formation|41210|5|Briefly described|Fig.3|||||||||
14635|Orallo Formation|41216|6|Mentioned|Fig.18|||||||||
14635|Orallo Formation|41246|6|Mentioned|Map legend|Jurassic||||||||
14635|Orallo Formation|41247|6|Mentioned|Fig.7|||||||||
14635|Orallo Formation|41266|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|41290|6|Mentioned|p227|||||||||
14635|Orallo Formation|41681|6|Mentioned|p7|||||||||
14635|Orallo Formation|41992|4|Described|Fig.2 P183|||||||||
14635|Orallo Formation|42007|5|Briefly described|Fig.2 P182|||||||||
14635|Orallo Formation|42463|6|Mentioned|Fig.5 P172|||See also Fig.6 P173||||||
14635|Orallo Formation|42493|5|Briefly described|p20, Fig. 1 p18|||||||||
14635|Orallo Formation|42494|5|Briefly described|Table 1 P24|||||||||
14635|Orallo Formation|42634|6|Mentioned|Table 8 P34|||||||||
14635|Orallo Formation|42679|6|Mentioned|Fig.3 P3|||||||||
14635|Orallo Formation|42950|6|Mentioned|p41|||||||||
14635|Orallo Formation|43000|5|Briefly described|Fig.5,p112|||Of Blythesdale Group.||||||13-MAR-09
14635|Orallo Formation|43002|5|Briefly described|Fig.2,p135|||||||||
14635|Orallo Formation|43404|14|Not recorded|Table p11||Late Jurassic|||||||
14635|Orallo Formation|43539|14|Not recorded|p398|||||||||
14635|Orallo Formation|43582|6|Mentioned|Fig.5,p16||Late Jurassic|||||||
14635|Orallo Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group.||||||
14635|Orallo Formation|43982|14|Not recorded|Map Legend||Late Jurassic|||||||
14635|Orallo Formation|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
14635|Orallo Formation|43994|14|Not recorded|Map Legend|||||||||
14635|Orallo Formation|43998|4|Described|p16,map|Cretaceous|Jurassic|||||||
14635|Orallo Formation|44021|14|Not recorded|p232,233,238|||||||||
14635|Orallo Formation|44023|6|Mentioned|Tb.3,p12|||||||||
14635|Orallo Formation|44028|14|Not recorded|Fig.2||Jurassic|See Strat Table.||||||
14635|Orallo Formation|44031|14|Not recorded|p10,11||Late Jurassic|||||||
14635|Orallo Formation|44084|14|Not recorded|p32(Tb)|Late Jurassic|Middle Jurassic|Surat Basin.||||||
14635|Orallo Formation|44091|14|Not recorded|p57||Late Jurassic|||||||
14635|Orallo Formation|44171|14|Not recorded|p194,197|||||||||
14635|Orallo Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
14635|Orallo Formation|44371|14|Not recorded|Map Legend||Jurassic|||||||
14635|Orallo Formation|44377|14|Not recorded|p1-8,11-2,19,21-2map||Late Jurassic|Name supersedes Fossil Wood Beds and Orallo Coal Measures.||||||
14635|Orallo Formation|44414|14|Not recorded|p114|Cretaceous|Jurassic|||||||
14635|Orallo Formation|44415|14|Not recorded|Fig.2,p23|||||||||
14635|Orallo Formation|44636|14|Not recorded|p167(Tb)||Late Jurassic|||||||
14635|Orallo Formation|44637|14|Not recorded|p287-291||Jurassic|||||||
14635|Orallo Formation|44786|14|Not recorded|p193-202||Early Jurassic|||||||
14635|Orallo Formation|45071|3|Fully described|Table 15|||||||||
14635|Orallo Formation|45110|2|Defined|p102|Late Jurassic|Late Jurassic|Formerly Orallo C.M.(Jensen,26),Fossil Wood Beds(Whitehouse).See P24.||||||
14635|Orallo Formation|46791|6|Mentioned|Fig.2|||||||||
14635|Orallo Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
14635|Orallo Formation|46984|6|Mentioned|Table 1|||||||||
14635|Orallo Formation|48919|6|Mentioned|Table 5|||See also P70||||||
14635|Orallo Formation|48920|6|Mentioned|Table 7|||Refers Day (1964)||||||
14635|Orallo Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
14635|Orallo Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
14635|Orallo Formation|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
14635|Orallo Formation|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|61000|5|Briefly described|p186 Fig. 4|Tithonian|Tithonian|Geological Province: Surat Basin.||||||
14635|Orallo Formation|61310|5|Briefly described|p34|Late Jurassic|Late Jurassic|Geological Province: in the Queensland part of Clarence-Moreton Basin. May be equivalent to the Grafton Formation.||||||
14635|Orallo Formation|61313|5|Briefly described|p99, p98 Fig. G10|Early Cretaceous|Late Jurassic|Flood plain, alluvial, meandering fluvial deposits. Together with Mooga Formation, conformably overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||
14635|Orallo Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Labile sandstone, carbonaceous siltstone, mudstone. Overlies Pilliga Sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8, p154 Fig. SU9.||||||07-FEB-11
14635|Orallo Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
14635|Orallo Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|63979|6|Mentioned|p40|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
14635|Orallo Formation|64197|6|Mentioned|p630 Fig.7|Early Cretaceous|Early Cretaceous|||||Underlies the Mooga Sandstone, overlies the Gubberamunda Sandstone.||
14635|Orallo Formation|64665|5|Briefly described|p53 Fig.2, p60, p62.|Early Cretaceous|Early Cretaceous|Surat Basin. Contains thin coals.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|64856|3|Fully described|p79, p94-97|Berriasian|Late Jurassic|Surat Basin. Of Day (1964). Previously the Orallo Coal Measures and Orallo Measures (Jensen, 1926), "Fossil Wood Stages or Series" (Reeves, 1947) and "Fossil Wood Beds" (Whitehouse, 1955). Type area near Bungeworgorai Creek, near the abandoned Orallo rail siding. Transitionally overlies the Gubberamunda Sandstone. Grades up into Southlands Formation. Age from palynofloral unit APK1. Max. thickness 306m. Friable medium to coarse-grained sandstone, lesser interbedded carbonaceous siltstone, silty mudstone, bentonite, coal.|| ||||29-NOV-17
14635|Orallo Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Gubberamunda Sandstone, Surat Basin.||||||
14635|Orallo Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
14635|Orallo Formation|65003|4|Described|p1, p6, p8, p13-15, p21, p25-26||Middle Jurassic|Of Surat Basin.  Fluvial sediments. Extensive clay deposits.||||Overlain by the Mooga Sandstone. ?Overlies the Injune Creek Group.|Variably-sorted, labile to sub-labile in part, calcareous and clayey sandstone, interbedded carbonaceous siltstone, mudstone, shale, minor coal, bentonite, conglomerate and fossil wood.|30-MAR-12
14635|Orallo Formation|65112|5|Briefly described|p323; p327; Fig 11 p324; Fig 15 p327|Jurassic|Jurassic|Non-marine, upward-fining clastic sedimentary rock. A package (Supersequence L) comprising a lower sand-rich part, followed by a shale-rich unit.||||Overlies Gubberamunda and Pilliga Sandstones; underlies Mooga Sandstone.||22-MAR-12
14635|Orallo Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies both the Gubberamunda Sandstone and the  Pilliga Sandstone, underlies the Mooga Sandstone.||||||
14635|Orallo Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
14635|Orallo Formation|65116|4|Described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Shows increase in interbedded silt and mud in the sandstone compared with Pilliga Sst. Underlies the Mooga Formation, Overlies both the Gubberamunda Sandstone and Pilliga Sandstone, Surat  Basin.||||||06-MAR-12
14635|Orallo Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 7-8, 13-14, 16-19|Early Cretaceous|Late Jurassic|Surat Basin. Lithic sandstone, mudstone, siltstone conglomerate and coal. Formationup to 270 m thick. Age: 140-149 Ma. Fission Track age: 100-140 Ma.||||||07-MAR-12
14635|Orallo Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Gubberamunda and Pilliga Sandstones. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|67133|5|Briefly described|p2, p5, p16-17, p19-21|Cretaceous|Cretaceous|26 samples of this unit were analysed by XRD and optical microscopy for this study. Mainly low energy overbank and swamp deposits. Consists of quartz (30-68%), K-feldspars (~7%) and plagioclase (up to 48%). Kaolinite (up to 22%) is the main clay mineral. The mixed-layer clays vary locally from smectite- to illite-rich.||||Conformably overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.|Friable, medium- to coarse-grained, partly calcareous sandstones with minor siltstone, mudstone and coal beds; bentonitic tuffs indicate contemporaneous volcanic activity.|
14635|Orallo Formation|67402|4|Described|p146 fig SRT3, p148|Barremian|Tithonian|Surat Basin. Deposited in a fluvial environment with local ponding. Approximately 226m thick. See also p154 fig SRT15/16, p156.||Blythesdale Group||Overlies the Gubberamunda Sandstone. Overlain by the Mooga Sandstone.|Sandstone with silty mudstone, bentonite and coal.|
14635|Orallo Formation|67669|5|Briefly described|p11|Late Jurassic|Late Jurassic|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Mooga Sandstone. Underlain by Gubberamunda Sandstone.||
14635|Orallo Formation|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Gubberamunda Sandstone and Pilliga Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|68004|5|Briefly described|p87, p174.|||Organic-rich: high TOC. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows. Forms a poor-quality seal for the Pilliga Sandstone.||||||
14635|Orallo Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluvial environment.||||Conformably overlies Pilliga Sandstone. Is overlain by Mooga Sandstone.|Medium-grained, sub-lithic sandstone and interbedded siltstone and mudstone; minor coal seams.|
14635|Orallo Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Early Cretaceous|Surat Basin (NSW and QLD). Contains plant macrofossils.||||Overlies Pilliga and Gubberamunda Sandstones. Is overlain by Mooga Sandstone|Interbedded sandstone and siltstone.|14-SEP-17
14635|Orallo Formation|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil and Southlands Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
14635|Orallo Formation|68576|5|Briefly described|Q_4: p3-4, p22, p24|Early Cretaceous|Late Jurassic|Surat Basin. Previously known as Fossil Wood beds because it contains petrified wood. Is mined for bentonite. Deposited in a lacustrine environment with periods of volcanic activity.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.|Friable, medium- to coarse-grained, sub-labile to labile sandstone, in part calcareous, and lesser interbedded carbonaceous siltstone, silty mudstone, bentonite and coal. Fossil wood and conglomerate beds are common in the sandstone.|
14635|Orallo Formation|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Late Jurassic|Fluvial deposits. A minor aquifer in the map area.||||Overlies Pilliga Sandstone. Is overlain by Mooga Sandstone.|Medium-grained, sub-lithic sandstone and interbedded siltstone and mudstone with minor coal.|
14635|Orallo Formation|69582|5|Briefly described|p36, p38|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Gubberamunda Sandstone. Overlain by the Mooga Sandstone.|Sandstone, mudstone.|
14635|Orallo Formation|69594|5|Briefly described|p519, p527, p537-539, p573|Valanginian|Berriasian|Day (1964); = Orallo Measures and Orallo Coal Measures of Jensen (1926); = Fossil Wood Stage or Series of Reeves (1947); = Fossil Wood beds of Whitehouse (1955) in his Blythesdale Group. Northern Surat Basin. 150-350m thick. Fluvial deposits with sporadic lacustrine and swamp conditions in the upper part; deposition punctuated by tuffs. The source of most of QLD's bentonite (derived from tuffs). RELATED UNITS (continued): Equivalent to Hooray Sandstone and upper Kumbarilla beds.||||Conformably and transitionally overlies Gubberamunda Sandstone. Is overlain conformably by Mooga Sandstone (locally disconformably). Grades into lower Southlands Formation. See COMMENTS for more.|Sublabile to labile sandstones, lesser interbedded carbonaceous siltstone, mudstone, bentonite and minor coal with some conglomerates interbedded with the sandstones.|
14635|Orallo Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
14635|Orallo Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
14635|Orallo Formation|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal.||||||
14635|Orallo Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Berriasian.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
14635|Orallo Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||||Overlies Gubberamunda and Pilliga Sandstones. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown as located in the Surat Basin, both Qld and NSW.||||Overlies Pilliga Sandstone and Gubberamunda Sandstone and underlies Mooga Sandstone||
14635|Orallo Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: 119, 146, 151-152, 168-172, 177-178, 191.||||||
14635|Orallo Formation|73193|6|Mentioned|p369|Valanginian|Berriasian|Surat Basin.||||Underlain by Gubberamunda Sandstone. Overlain by Mooga Sandstone.||
14646|Orient beds|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
14646|Orient beds|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt Province; Leichhardt River Subprovince.||||||07-NOV-08
14646|Orient beds|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone. siltstone, conglomerate, calcareous rocks, ?volcanics. In the Kalkadoon-Leichardt Belt near Mount Isa.||||||09-FEB-09
14646|Orient beds|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Post-Barramundi basement. Marble shown as informal subdivision.||Of Leichhardt Volcanics.|||Quartzite, calcareous quartzite, metasiltstone, labile sandstone, conglomerate, marble and possible felsic to mafic volcanic rocks.|
14717|Owl Gully Volcanics|22973|5|Briefly described|p9 Fig.2 (a)|Early Permian|Early Permian|||||||
14717|Owl Gully Volcanics|23037|6|Mentioned|p48||Early Permian|||||||
14717|Owl Gully Volcanics|23468|5|Briefly described|Fig 2 p 295|||||||||
14717|Owl Gully Volcanics|24076|5|Briefly described|p397 Fig. 2|Late Permian|Early Permian|Max. thickness: 1525m.  Geological Province: Yarrol Basin.||||||
14717|Owl Gully Volcanics|24488|5|Briefly described|Map Legend|Permian|Permian|||||||
14717|Owl Gully Volcanics|24491|5|Briefly described|p14, p21|Early Permian|Namurian|||||||
14717|Owl Gully Volcanics|24615|5|Briefly described|CD|Permian|Permian|[Pvo].  Andesitic lava, lithic sandstone, siltstone.||||||
14717|Owl Gully Volcanics|30450|6|Mentioned|Table 1|||Permian age. Yarrol Basin||||||
14717|Owl Gully Volcanics|30451|4|Described|p41|||Permian age.||||||19-AUG-08
14717|Owl Gully Volcanics|30914|6|Mentioned|Map legend|Permian|Permian|||||||
14717|Owl Gully Volcanics|33774|6|Mentioned|p30|||Correlation||||||
14717|Owl Gully Volcanics|34132|6|Mentioned|p4|||Lower Permian||||||
14717|Owl Gully Volcanics|34138|6|Mentioned|Cor.Chart|||Artinskian||||||
14717|Owl Gully Volcanics|34408|6|Mentioned|p185|||On Table||||||
14717|Owl Gully Volcanics|37109|5|Briefly described|p283|||||||||
14717|Owl Gully Volcanics|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
14717|Owl Gully Volcanics|39252|6|Mentioned|p21|||||||||
14717|Owl Gully Volcanics|39445|5|Briefly described|Table 8|||||||||
14717|Owl Gully Volcanics|40623|5|Briefly described|p79|||||||||
14717|Owl Gully Volcanics|41246|6|Mentioned|Map legend|Permian||||||||
14717|Owl Gully Volcanics|43017|5|Briefly described|Fig.3,p375|||||||||
14717|Owl Gully Volcanics|43883|14|Not recorded|p18 Fig.4-3|||||||||
14717|Owl Gully Volcanics|43998|14|Not recorded|Map||Early Permian|||||||
14717|Owl Gully Volcanics|44091|14|Not recorded|p47,Tb.3||Early Permian|||||||
14717|Owl Gully Volcanics|44369|2|Defined|Tb.6,p169,171||Early Permian|Basalt and andesite.||||||
14717|Owl Gully Volcanics|44370|14|Not recorded|p217,219,Tb.7|||||||||
14717|Owl Gully Volcanics|44378|14|Not recorded|p199|||Fauna of straight nautiloids.||||||
14717|Owl Gully Volcanics|44379|4|Described|p1,2,18-21,24,25,map||Early Permian|||||||
14717|Owl Gully Volcanics|44381|14|Not recorded|p9|||||||||
14717|Owl Gully Volcanics|44388|14|Not recorded|p113|||Equivalent overlies Dinner Creek Conglomerate.||||||
14717|Owl Gully Volcanics|50214|5|Briefly described|Map Legend|Early Triassic|Late Permian|||||||
14717|Owl Gully Volcanics|61772|6|Mentioned|p128 Fig. 2||Early Permian|In text, Volcanics is V.. In New England Orogen.||||||
14717|Owl Gully Volcanics|63600|5|Briefly described|p900 Fig. 1, p919|Early Permian|Early Permian|Age equivalent of Rookwood Volcanics. Ranges from basalt to andesite.||||||07-FEB-11
14717|Owl Gully Volcanics|63832|6|Mentioned|p131 fig 2|Artinskian|Artinskian|Of east Bowen Basin.||||||
14717|Owl Gully Volcanics|64399|5|Briefly described|Map legend|Early Permian|Early Permian|Andesitic lava, lithic sandstone, siltstone.||||||
14717|Owl Gully Volcanics|64631|5|Briefly described|p44 Fig.2.|Artinskian|Artinskian|?Northern New England Fold Belt. Biostratigraphic age control for base and top.||||Overlies Yarrol Formation.||
14717|Owl Gully Volcanics|65388|6|Mentioned|p35, 39, 43, 55|||Yarrol Syncline SE of Monto. May correlate with Yaparaba Volcanics, Nogo beds. Equivalent age to Rookwood Volcanics.||||||
14717|Owl Gully Volcanics|68008|3|Fully described|p2, p106, p134-144, p147, p153, p157|Permian|Permian|See also p483, p491, p569. Maxwell (1959). The type area is on the E limb of the Yarrol Syncline, W of Yarrol homestead. Monto district. Two areas mapped by Dear et al. (1971) have been reassigned (described). Forms rugged hilly topography. Geochemistry detailed, REE and spidergram plots: strong subduction signature. 1500m thick. Artinskian age. Youngest unit folded in the Yarrol Syncline.|c.280-275 Ma.|||Conformably overlies Yarrol Formation. Probable correlative of the Smoky beds. May be partial time equivalent of Berserker group, Rookwood Volcanics, Narayen beds, Nogo beds and Buffel Formation.|Characterised by andesite lava: dark, commonly vesicular; interbedded black or brownish-black siltstones, calcareous when fresh; associated lithic sandstones.|
14717|Owl Gully Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Yarrol Province. This unit, with the Inverness Volcanics and unnamed volcanic units, are all mapped under the symbol, Pvo.||||||
14717|Owl Gully Volcanics|68679|5|Briefly described|p312-313, p337-338, p342-344, p352, p380|Cisuralian|Cisuralian|See also p469-470. Maxwell (1959). Monto area, Yarrol Syncline, northern New England Orogen. 1500m or so thick. Has a strong subduction signature. Some rocks mapped as this unit by Dear et al. (1971) have been assigned to the Smoky beds.||||Probably correlated with Nogo beds.|Amygdaloidal and porphyritic andesite lava flows; interbedded siltstone is calcareous and graded, or poorly bedded with angular black siltstone clasts; associated calcareous lithic sandstone is commonly graded, with subangular andesitic fragments.|
14717|Owl Gully Volcanics|73197|6|Mentioned|p474, p475 Fig.6, p478|Lopingian|Guadalupian|New England Orogen, northern. Coeval with Rookwood Volcanics, Berserker Group, Double Mountain Volcanics, Peninsula Range Volcanics. Strong subduction geochemical signature (Murray et al., 2012).|||||Andesitic lavas and pyroclastics.|
14721|Oxley Group|33368|6|Mentioned|p49|||||||||
14721|Oxley Group|33881|5|Briefly described|p96|||||||||
14721|Oxley Group|36237|6|Mentioned|Map legend|Tertiary|Tertiary|Located in back pocket.||||||
14721|Oxley Group|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14721|Oxley Group|37375|4|Described|p476|||||||||
14721|Oxley Group|38074|5|Briefly described|Table 1|||||||||
14721|Oxley Group|38307|6|Mentioned|Fig.1|||||||||
14721|Oxley Group|38441|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
14721|Oxley Group|39445|6|Mentioned|Table 14|||||||||
14721|Oxley Group|40623|5|Briefly described|p8|||||||||
14721|Oxley Group|41906|3|Fully described|Table 4 P34|||||||||
14721|Oxley Group|42525|5|Briefly described|Map legend|Miocene|Paleocene|||||||
14721|Oxley Group|43008|5|Briefly described|map legend|||||||||
14721|Oxley Group|43076|5|Briefly described|p11|||||||||
14721|Oxley Group|44687|1|Redefined|p225,226|||Redefinition of Oxley Beds.  Consists of Darra, Corinda and Sunnybank Formations.||||||
14721|Oxley Group|44703|14|Not recorded|Map||Tertiary|||||||
14721|Oxley Group|44708|14|Not recorded|p5,Sh.1-3,section||Tertiary|||||||
14721|Oxley Group|61155|5|Briefly described|p19|Middle Eocene|Late Paleocene|Comprises Darra, Corinda and Sunnybank Formations. In the Brisbane region.||||||
14721|Oxley Group|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Booval Group; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
14721|Oxley Group|69599|5|Briefly described|p586, p594-595|Eocene|Eocene|Houston (1965). Oxley Basin. All three Formations are present only in the north, due to pre-existing topography; cannot be subdivided south of Carole Park. Capped by laterite.|||Darra, Corinda, Sunnybank Formations.|Unconformably overlies the Neranleigh-Fernvale beds. Lower part correlated with Booval Group.||
14723|Oxtrack Formation|13516|5|Briefly described|p145 fig 3|Late Permian|Late Permian|From Taroom Shelf, Bowen Basin. Age: APP5002 - APP5003.||||||
14723|Oxtrack Formation|22439|5|Briefly described|p15, Fig.2|Late Permian|Early Permian|Taroom Trough, Bowen Basin.||||||
14723|Oxtrack Formation|22973|5|Briefly described|p9 Fig.2 (d)|Late Permian|Late Permian|||||||
14723|Oxtrack Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
14723|Oxtrack Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
14723|Oxtrack Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
14723|Oxtrack Formation|23037|4|Described|p40,53,60,4,5,6,7,9,128||Early Permian|Possible equivalent to Buffel Formation.  Underlying unit Woolein beds.||||||
14723|Oxtrack Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
14723|Oxtrack Formation|24552|5|Briefly described|p27|Kungurian|Kungurian|Contains bryozoans, some described here. Geological Province: Bowen Basin. QLD.||||||07-FEB-11
14723|Oxtrack Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pbo].  Silty limestone, limestone, calcareous siltstone, mudstone, siltstone, sandstone.||||||
14723|Oxtrack Formation|29437|6|Mentioned|p136|||Permian||||||
14723|Oxtrack Formation|29440|6|Mentioned|p38|||Permian brachiopods||||||
14723|Oxtrack Formation|30141|5|Briefly described|p134|||||||||
14723|Oxtrack Formation|30449|6|Mentioned|p8|||Brachiopods. See also P21||||||
14723|Oxtrack Formation|30450|6|Mentioned|Table 1|||Permian age. Southeast Bowen Basin||||||
14723|Oxtrack Formation|30451|4|Described|p52|||||||||
14723|Oxtrack Formation|30546|6|Mentioned|p107|||Upper Permian age. See also P111.||||||15-JUL-13
14723|Oxtrack Formation|30743|6|Mentioned|p24|||Geological map||||||
14723|Oxtrack Formation|31079|6|Mentioned|Fig. 6|||||||||
14723|Oxtrack Formation|31396|6|Mentioned|p1185|||||||||
14723|Oxtrack Formation|31531|5|Briefly described|p8|||See also Table 1.||||||
14723|Oxtrack Formation|31656|4|Described|Table 1|||||||||
14723|Oxtrack Formation|31659|6|Mentioned|p106|||||||||
14723|Oxtrack Formation|32141|6|Mentioned|p154|||||||||
14723|Oxtrack Formation|32496|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14723|Oxtrack Formation|32577|6|Mentioned|p23|||Blenheim Sub Gp.||||||
14723|Oxtrack Formation|32944|6|Mentioned|Fig.3|||See also P704. Permian||||||
14723|Oxtrack Formation|32945|6|Mentioned|p90|||See also P91. Permian||||||
14723|Oxtrack Formation|33436|6|Mentioned|p241|||Fauna.||||||
14723|Oxtrack Formation|33774|3|Fully described|p35|||||||||
14723|Oxtrack Formation|34132|6|Mentioned|p2|||Upper Permian||||||
14723|Oxtrack Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
14723|Oxtrack Formation|34348|6|Mentioned|p20|||Upper Permian||||||
14723|Oxtrack Formation|34568|6|Mentioned|p223|||||||||
14723|Oxtrack Formation|35145|6|Mentioned|p83|||||||||
14723|Oxtrack Formation|35284|6|Mentioned|Fig.1|||||||||
14723|Oxtrack Formation|35426|3|Fully described|p656|||||||||
14723|Oxtrack Formation|35845|6|Mentioned|Fig.25|||||||||
14723|Oxtrack Formation|35862|6|Mentioned|p272|||||||||
14723|Oxtrack Formation|35873|6|Mentioned|Fig.38|||||||||
14723|Oxtrack Formation|36045|6|Mentioned|p333|||||||||
14723|Oxtrack Formation|36243|6|Mentioned|Table 4A|||||||||
14723|Oxtrack Formation|36333|6|Mentioned|Map legend|Late Permian|Late Permian|Of the Back Creek Group.||||||15-JUL-04
14723|Oxtrack Formation|36739|6|Mentioned|Fig.2|||||||||
14723|Oxtrack Formation|36925|6|Mentioned|p179|||||||||
14723|Oxtrack Formation|37075|5|Briefly described|Table 1|||||||||
14723|Oxtrack Formation|37858|6|Mentioned|Fig.1|||||||||
14723|Oxtrack Formation|38153|6|Mentioned|p373|||||||||
14723|Oxtrack Formation|38204|4|Described|p75|||||||||
14723|Oxtrack Formation|38444|6|Mentioned|p302|||||||||
14723|Oxtrack Formation|38447|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14723|Oxtrack Formation|39212|5|Briefly described|p12|||||||||
14723|Oxtrack Formation|39261|6|Mentioned|Fig.6|||||||||
14723|Oxtrack Formation|39267|6|Mentioned|p236|||||||||
14723|Oxtrack Formation|39445|5|Briefly described|Table 8|||||||||
14723|Oxtrack Formation|39943|6|Mentioned|Table 6A|||||||||
14723|Oxtrack Formation|40091|6|Mentioned|p72|||||||||
14723|Oxtrack Formation|40093|4|Described|p30|||||||||
14723|Oxtrack Formation|40539|6|Mentioned|Fig.2|||||||||
14723|Oxtrack Formation|41246|6|Mentioned|Map legend|Permian||||||||
14723|Oxtrack Formation|41546|4|Described|p157|||||||||
14723|Oxtrack Formation|41639|6|Mentioned|p7|||||||||
14723|Oxtrack Formation|41666|6|Mentioned|P|||||||||
14723|Oxtrack Formation|41809|6|Mentioned|p75|||||||||
14723|Oxtrack Formation|42249|6|Mentioned|p22|||||||||
14723|Oxtrack Formation|42250|6|Mentioned|Fig.3 P30|||||||||
14723|Oxtrack Formation|42540|6|Mentioned|p315|||||||||
14723|Oxtrack Formation|43000|5|Briefly described|p111|||see also Fig.5,p112||||||
14723|Oxtrack Formation|43017|5|Briefly described|Fig.3,p375|||||||||
14723|Oxtrack Formation|43050|5|Briefly described|p4|||||||||
14723|Oxtrack Formation|43185|6|Mentioned|6,9||Late Permian|||||||
14723|Oxtrack Formation|43474|14|Not recorded|p60|||Permian fossils||||||
14723|Oxtrack Formation|43475|14|Not recorded|p553||Permian|||||||
14723|Oxtrack Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
14723|Oxtrack Formation|43987|14|Not recorded|p267,270|||||||||
14723|Oxtrack Formation|43994|14|Not recorded|Map Legend|||||||||
14723|Oxtrack Formation|43995|14|Not recorded|Tb.p9|Permian|Carboniferous|||||||
14723|Oxtrack Formation|44118|14|Not recorded|Map Legend||Late Permian|||||||
14723|Oxtrack Formation|44169|2|Defined|Tb.1,p8,map|||||||||
14723|Oxtrack Formation|44170|4|Described|p7-9,11,31,Tb.1,map||Late Permian|||||||
14723|Oxtrack Formation|44218|14|Not recorded|p19||Sakmarian|||||||
14723|Oxtrack Formation|44243|14|Not recorded|p649,map||Late Permian|||||||
14723|Oxtrack Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
14723|Oxtrack Formation|44380|14|Not recorded|p94|||||||||
14723|Oxtrack Formation|44381|14|Not recorded|p5-6|||||||||
14723|Oxtrack Formation|44382|14|Not recorded|p112|||||||||
14723|Oxtrack Formation|44424|14|Not recorded|p293-301|||||||||
14723|Oxtrack Formation|44426|14|Not recorded|p11|||Transgressive.||||||
14723|Oxtrack Formation|44427|1|Redefined|p159-162,164,165|Kazanian|Kungurian|Now limited to Kungurian-Kazanian, remainder becomes Buffel Formation. Equivalent to lower Peawaddy Formation. Mundubbera area.||||||
14723|Oxtrack Formation|44490|14|Not recorded|p48|||Fossils.||||||
14723|Oxtrack Formation|44514|2|Defined|p27,28||Artinskian|Basal formation of Back Creek Group. Overlies Camboon Andesite. Conformably overlain by Orange Creek Formation.||||||
14723|Oxtrack Formation|44571|2|Defined|p205,206,Fig.28||Early Permian|||||||
14723|Oxtrack Formation|44640|14|Not recorded|p30|||||||||
14723|Oxtrack Formation|45006|14|Not recorded|Tb.1,p3,103|||||||||
14723|Oxtrack Formation|45031|14|Not recorded|p9,11,25,32,89,102,||Permian|p106,114,120,122,128,Fig.3,Pl.1-4,8,11,12,15,18||||||
14723|Oxtrack Formation|45071|3|Fully described|Table 10|||See also P54||||||
14723|Oxtrack Formation|46949|6|Mentioned|Fig.3|||||||||
14723|Oxtrack Formation|48898|5|Briefly described|p1|||See also PP15,25,27 etc. U.Permian||||||
14723|Oxtrack Formation|48900|6|Mentioned|p84|||Table opposite.||||||
14723|Oxtrack Formation|48919|4|Described|p21|||U.Permian. See also P22||||||
14723|Oxtrack Formation|48926|6|Mentioned|p49|||pp49 et seq.||||||15-JUL-13
14723|Oxtrack Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Back Creek Group. Silty limestone, limestone, calcareous siltstone, mudstone, siltstone and lithic siltstone.||||||18-JUN-09
14723|Oxtrack Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Back Creek Group. Silty limestone, limestone, calcareous siltstone, mudstone, siltstone and lithic sandstone.||||||
14723|Oxtrack Formation|50301|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Back Creek Group.||||||
14723|Oxtrack Formation|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Back Creek Group.||||||
14723|Oxtrack Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province:  eastern margin Bowen Basin.||||||04-FEB-08
14723|Oxtrack Formation|60282|5|Briefly described|p7|Late Permian|Late Permian|Overlain by Barfield Formation.  Separated from the underlying lithologically similar Early Permian Buffel Formation by a disconformity.  Geological Province: Bowen Basin.||||||
14723|Oxtrack Formation|61076|5|Briefly described|p188 Fig. 2|Permian|Permian|Age: >260Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
14723|Oxtrack Formation|61782|6|Mentioned|p280|||Of Blenheim Subgroup. Contains carbonates.||||||
14723|Oxtrack Formation|62357|6|Mentioned|p524 Fig. 7, p528|Middle Permian|Middle Permian|Geological Province: Bowen Basin (Taroom Trough).||||||
14723|Oxtrack Formation|64856|4|Described|p51-52, p102|Late Permian|Late Permian|Derrington et al. (1959). Type area is Oxtrack Creek, N of Cracow. Redefined by Wass (1965) and Flood et al. (1981). Bowen Basin. Fossiliferous limestone and calcareous shale. An interval in Cockatoo Creek 1, formerly assigned to this unit, is now considered to be part of the Barfield Formation.|| ||||29-NOV-17
14723|Oxtrack Formation|64857|5|Briefly described|p116,118, p113 Fig.3|||Bowen Basin. Fossiliferous limestones and calcareous siltstones and sandstones. Overlies Buffel Formation.||||||
14723|Oxtrack Formation|64858|6|Mentioned|p180 Fig.2|Late Permian|Early Permian|||||||30-NOV-09
14723|Oxtrack Formation|65112|6|Mentioned|p316; p321; Fig 4 p314|Triassic|Late Permian|Post-extension stratigraphic sequences of the Taroom Trough. Underlies Barfield Formation.||||||22-MAR-12
14723|Oxtrack Formation|65113|5|Briefly described|p345, p347, Fig 4 p340|Late Permian|Early Permian|Taroom Trough. Underlies the Barfield Formation, but there is a gap in the rock record from ~280-265 Ma.||||||
14723|Oxtrack Formation|65114|5|Briefly described|p385 Fig.3|Late Permian|Early Permian|||||||
14723|Oxtrack Formation|65115|5|Briefly described|p413, Fig 2 p403|Ufimian|Kungurian|Underlies the Barfield Formation in the Taroom Trough, Bowen Basin. Part of Supersequence C.||||||
14723|Oxtrack Formation|65116|5|Briefly described|p444, fig 2 p436|Late Permian|Late Permian|Underlies the Barfield Formation in the Taroom Trough, Bowen Basin.||||||19-MAR-13
14723|Oxtrack Formation|65118|6|Mentioned|p491, Fig 2 p479|Permian|Permian|Underlies the Barfield Formation in the Taroom Trough, Bowen Basin.||||||
14723|Oxtrack Formation|65119|6|Mentioned|Fig 4 p510, Fig 5 p511|||Present in the Cockatoo Creek Well.||||||
14723|Oxtrack Formation|65388|4|Described|p165-167; p167, 31, 32, 48, 70, 159-161|Late Permian|Kungurian|Of Back Creek Group, Bowen Basin. Defined by Derrington and others (1959). Redefined Wass (1965). Overlies Buffel Formation, Camboon Volcanics, Woolein beds. Includes rocks described as Brae Formation by Flood et al (1981), Briggs (1993) and others.  Overlain conformably by the Barfield Formation.  Characterised by grey bioclastic limestone, fossiliferous silty limestone, siltstone, mudstone and lithic sandstone. Limestones dominated by skeletal grainstones. Distinctive fauna indicates Kungurian age. Spores-pollen indicate an age not older than lower stage 5b (Ufimian or early Kazanian). See also p163, 174, 179.||||||
14723|Oxtrack Formation|66615|6|Mentioned|p2 Fig.1, p9|||Southern Taroom Trough, Bowen Basin.||||||
14723|Oxtrack Formation|67402|6|Mentioned|p21, p45|Capitanian|Wordian|Bowen Basin.||||Overlain by the Banana, Flat Top and Barfield Formations. Unconformably overlies the Buffel Formation.||
14723|Oxtrack Formation|67669|5|Briefly described|p11|Early Permian|Early Permian|Of Bowen Basin.||||Overlain by Barfield Formation. Underlain by Buffel Formation.||
14723|Oxtrack Formation|68679|5|Briefly described|p353, p375, p378, p380-381|Permian|Permian|Derrington et al. (1959). Connors-Auburn Province. SE Bowen Basin. 400m thick. Marine shelf deposits.||||Unconformably overlies Buffel Formation. Is overlain by Barfield Formation.|Fossiliferous (skeleton) limestone, calcareous siltstone, siltstone and sandstone.|
14723|Oxtrack Formation|73450|6|Mentioned|p55|||Bowen Basin.||||||
14735|Packsaddle Microgranite|23065|6|Mentioned|13|Proterozoic|Proterozoic|||||||
14735|Packsaddle Microgranite|23363|5|Briefly described|352 Table 3|Statherian|Statherian|Age: 1724+/-4Ma.||||||26-MAR-18
14735|Packsaddle Microgranite|23395|6|Mentioned|p395|||||||||
14735|Packsaddle Microgranite|23396|6|Mentioned|p423 Fig.17|||||||||
14735|Packsaddle Microgranite|23397|6|Mentioned|p464 Fig.3|||||||||
14735|Packsaddle Microgranite|23398|4|Described|p437|Statherian|Statherian|Age: 1724+/-4Ma.||||||22-NOV-06
14735|Packsaddle Microgranite|24048|6|Mentioned|p36|||Geological Province: McArthur Basin.||||||
14735|Packsaddle Microgranite|24050|6|Mentioned|p30|||||||||
14735|Packsaddle Microgranite|32519|6|Mentioned|p341|||||||||
14735|Packsaddle Microgranite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|32660|6|Mentioned|p222|||||||||
14735|Packsaddle Microgranite|32904|6|Mentioned|p95|||||||||
14735|Packsaddle Microgranite|34811|6|Mentioned|Fig.2|||||||||
14735|Packsaddle Microgranite|35114|6|Mentioned|p204|||||||||
14735|Packsaddle Microgranite|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|35776|4|Described|p819|||||||||
14735|Packsaddle Microgranite|35950|6|Mentioned|p312|||||||||
14735|Packsaddle Microgranite|36012|6|Mentioned|Fig.2|||||||||
14735|Packsaddle Microgranite|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14735|Packsaddle Microgranite|37217|6|Mentioned|p650|||||||||
14735|Packsaddle Microgranite|37371|6|Mentioned|p368|||||||||
14735|Packsaddle Microgranite|37462|6|Mentioned|p244|||||||||
14735|Packsaddle Microgranite|37565|6|Mentioned|p11|||||||||
14735|Packsaddle Microgranite|39445|5|Briefly described|Table 2|||Age p39. See also p36.||||||22-NOV-06
14735|Packsaddle Microgranite|40691|5|Briefly described|p11|||||||||
14735|Packsaddle Microgranite|40811|6|Mentioned|p318|||||||||
14735|Packsaddle Microgranite|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
14735|Packsaddle Microgranite|41721|3|Fully described|p25||Paleoproterozoic|Of the Tawallah Group. Overlain by McArthur Group rocks. Intrudes Wollogorong Formation and Gold Creek Volcanics. Age: 1690Ma.  Porphyritic microgranite.||||||07-NOV-08
14735|Packsaddle Microgranite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
14735|Packsaddle Microgranite|41957|6|Mentioned|p68|||||||||
14735|Packsaddle Microgranite|43715|6|Mentioned|p28|||||||||
14735|Packsaddle Microgranite|44112|6|Mentioned|p43|||||||||
14735|Packsaddle Microgranite|44305|14|Not recorded|p.13,18|||(E53-8). opp.6,18.||||||
14735|Packsaddle Microgranite|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
14735|Packsaddle Microgranite|44436|5|Briefly described|p.12-13,opp. p.7,map|||Intrusive equivalent of Hobblechain Rhyolite Member. (E53-4).||||||02-DEC-04
14735|Packsaddle Microgranite|44437|5|Briefly described|map legend|Precambrian|Precambrian|Porphyritic microgranite.||||||08-DEC-04
14735|Packsaddle Microgranite|45087|5|Briefly described|p16|||Chemical analyses||||||
14735|Packsaddle Microgranite|45162|2|Defined|p44|Proterozoic|Proterozoic|Reference area location given.||||||22-FEB-18
14735|Packsaddle Microgranite|46919|6|Mentioned|p221|||||||||
14735|Packsaddle Microgranite|48894|6|Mentioned|p24|||Age: 1520my.||||||22-NOV-06
14735|Packsaddle Microgranite|50591|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Fagan Supersuite. Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
14735|Packsaddle Microgranite|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
14735|Packsaddle Microgranite|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Red, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic microgranite. Intrudes the Gold Creek Volcanics.||||||07-NOV-08
14735|Packsaddle Microgranite|63112|6|Mentioned|p1192 Tb.1|||Calvert Superbasin. May have been feeder fissure for Hobblechain Rhyolite.|1724 +/- 4 Ma.||||Porphyritic rhyolite with quartz phenocrysts and microgranophyric to spherulitic texture.|
14735|Packsaddle Microgranite|64817|6|Mentioned|p370|||||||||
14735|Packsaddle Microgranite|65228|5|Briefly described|Figs.06, 07, 10.|Statherian|Statherian|Southern McArthur Basin.|1724 +/- 4 Ma (Page et al.2000).|||Intrudes Tawallah Group.||
14735|Packsaddle Microgranite|65337|6|Mentioned|p17.|||Southeastern McArthur Basin.|c.1725 Ma.|||||
14735|Packsaddle Microgranite|65340|3|Fully described|p11, p13 Table 4, pp46-47.|||A small (70 sq. km. outcrop) high-level, elongate northwest-striking laccolith. Chemically indistinguishable from the central, massive portion of Hobblechain Rhyolite, for which it was probably the feeder.|1724 +/- 4 Ma (Page et al. 2000).|Unit in Tawallah Group.||Intrudes Wollogorang Formation and Gold Creek Volcanics. Contiguous and co-magmatic with Hobblechain Rhyolite.|Red or pink, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic rhyolite and microgranite. Quartz veins common.|26-MAR-18
14735|Packsaddle Microgranite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p107|Paleoproterozoic|Paleoproterozoic|Weberra Igneous Event. Shown informally as Packsaddle microgranite on p9.|||||Feldspar porphyry|
14735|Packsaddle Microgranite|67352|6|Mentioned|p14 Tb.2|||||||Intrudes Gold Creek Volcanics.||
14735|Packsaddle Microgranite|69430|4|Described|p15:9-10, 48|||Southern McArthur Basin. High-level laccolith: comagmatic with Hobblechain Rhyolite. Mineralised breccia pipes in the Running Creek area are contemporaneous with this unit.|1725 +/- 2 Ma (Page and Sweet, 1998).|Tawallah Group.||Intrudes Wollogorang Formation and Gold Creek Volcanics. Contiguous with Hobblechain Rhyolite.|Red or pink, porphyritic (K-feldspar-quartz), microgranophyric to spherulitic rhyolite and microgranite.|12-JUL-16
14735|Packsaddle Microgranite|69591|5|Briefly described|p38, p59|||N of the Murphy Tectonic Ridge. Has chemical and lithological similarities to the Peters Creek Volcanics.|1724 +/- 4 Ma.||||Feldspar porphyry.|
14735|Packsaddle Microgranite|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.|||Pink, porphyritic microgranite.|
14735|Packsaddle Microgranite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1724+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Quartz-feldspar microgranite, ferruginised.|
14735|Packsaddle Microgranite|72526|5|Briefly described|p6 Fig.1.2.|Paleoproterozoic|Paleoproterozoic|||||||
14735|Packsaddle Microgranite|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||Tawallah Group||Underlain by Gold Creek Volcanics. Overlain by Warramana Sandstone[?]. Equivalent to Hobblechain Rhyolite and Pungalina Member.||
14735|Packsaddle Microgranite|73083|6|Mentioned|p37, p40|||A tiny intrusion that intrudes the McArthur Basin sequence.||||||
14759|Paddys Creek Phyllite|23032|5|Briefly described|p12,14||Early Paleozoic|||||||07-NOV-08
14759|Paddys Creek Phyllite|23291|4|Described|p27, p82 Tb. 3.6p|Ordovician|Cambrian|Of the Lucky Creek Metamorphic Group. Geological Province: Georgetown Region.||||||08-JUL-15
14759|Paddys Creek Phyllite|23424|5|Briefly described|p345|||May correlate with quartzose turbidite units in the Broken River Province.||||||21-JUN-13
14759|Paddys Creek Phyllite|23430|5|Briefly described|p469|||Of Lucky Metamorphic Group. Thalanga Province.||||||16-FEB-09
14759|Paddys Creek Phyllite|23619|4|Described|p35 Table 1||Early Paleozoic|Strongly deformed. Also see p6. Of Lucky Creek Metamorphic Group. Underlain by Eland Metavolcanics. Georgetown Province.||||||16-FEB-09
14759|Paddys Creek Phyllite|24577|6|Mentioned|p755 Fig. 2|Early Paleozoic|Proterozoic|||||||07-NOV-08
14759|Paddys Creek Phyllite|41675|1|Redefined|p53|Paleozoic||Modified name of Paddys Creek Formation.||||||16-FEB-09
14759|Paddys Creek Phyllite|41975|5|Briefly described|p439|||||||||
14759|Paddys Creek Phyllite|42054|6|Mentioned|p273|||||||||
14759|Paddys Creek Phyllite|42279|4|Described|p17|||See also Fig.2||||||
14759|Paddys Creek Phyllite|42407|5|Briefly described|p34|||Compare with Paddys Creek Formation, p33.||||||16-FEB-09
14759|Paddys Creek Phyllite|42692|5|Briefly described|map legend|Ordovician|Cambrian|||||||
14759|Paddys Creek Phyllite|42693|5|Briefly described|map legend|Early Paleozoic|Proterozoic|||||||07-NOV-08
14759|Paddys Creek Phyllite|43113|4|Described|Table 1 p21|||Early Palaeozoic (Ordovician?). Of Lucky Creek Metamorphic Group.||||||17-JUL-14
14759|Paddys Creek Phyllite|43253|5|Briefly described|map legend|Ordovician|Cambrian|||||||
14759|Paddys Creek Phyllite|43286|5|Briefly described|Map Legend|Ordovician|Cambrian|||||||
14759|Paddys Creek Phyllite|50202|5|Briefly described|Map legend|Early Ordovician|Cambrian|Phyllite and quartzite.||||||
14759|Paddys Creek Phyllite|67455|4|Described|p575 Table 1, p576, p577, p584 Fig.7.|Ordovician|Cambrian|Constitutes the Paddys Creek domain, Greenvale Province. Has a more complex structural history than other units in the Lucky Creek Metamorphic Group: four main deformations and abundant mesoscopic F3 folds; but only greenschist facies metamorphism.||Unit in Lucky Creek Metamorphic Group.|||Pelite; lesser quartzite.|
14759|Paddys Creek Phyllite|68336|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Lucky Creek Metamorphic Group.|||Phyllite and quartzite; locally mylonitic.|
14759|Paddys Creek Phyllite|68341|5|Briefly described|Map legend.|Early Ordovician|Late Cambrian?|Cape River Province.||Unit in Lucky Creek Metamorphic Group.|||Phyllite and quartzite; locally mylonitic.|
14759|Paddys Creek Phyllite|68344|5|Briefly described|Map legend.|Early Ordovician|Cambrian|Thalanga Province. Weakly to non-magnetic.|||||Phyllite and quartzite; locally mylonitic.|
14759|Paddys Creek Phyllite|68480|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Thalanga Province. Late Cambrian? maximum age.|||||Phyllite and quartzite; locally mylonitic.|
14759|Paddys Creek Phyllite|68481|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Thalanga Province. Late Cambrian? maximum age.|||||Phyllite and quartzite; locally mylonitic.|
14759|Paddys Creek Phyllite|68576|5|Briefly described|Q_11: p33-35|||Age and relationships uncertain; probably Cambrian or Ordovician; may be correlative  of Seventy Mile Range Group.||Lucky Creek Metamorphic Group.||||
14759|Paddys Creek Phyllite|68731|5|Briefly described|p151 Fig 3.51, p153 Fig 3.52, p158|Ordovician|Ordovician|No age constraints for this unit have been determined.||Of the Lucky Creek Metamorphic Group.||Overlain and underlain by the Eland Metavolcanics.|Comprises mainly phyllite and lesser quartzite derived from mudstone and quartzose sandstone.|17-JUL-14
14815|Pandora Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 426. I-Type.||||||
14815|Pandora Granite|23713|5|Briefly described|p72 Appendix 2|||Intrudes Hodgkinson Formation. I-type granite. Of Ootann Supersuite.||||||
14815|Pandora Granite|42681|4|Described|p20|||||||||
14815|Pandora Granite|43083|5|Briefly described|p255|||Of Ootann Supersuite. I-type.  Lithology included.||||||17-JUN-09
14815|Pandora Granite|43087|2|Defined|p91|Early Permian|Late Carboniferous|||||||
14815|Pandora Granite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Ootann Suite. Pale pink to white, fine-grained, sparsely porphyritic biotite leucogranite to aplite.||||||15-JUN-06
14815|Pandora Granite|43254|5|Briefly described|map legend|Early Permian|Late Carboniferous|of Ootann Supersuite.Age Late Carboniferous to Early Permian?||||||
14815|Pandora Granite|43259|4|Described|Appendix 1,p46.|Permian|Carboniferous|||||||
14815|Pandora Granite|43625|6|Mentioned|p21|||||||||
14815|Pandora Granite|43626|6|Mentioned|p11||Late Carboniferous|||||||
14815|Pandora Granite|50316|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Geological Province: Kennedy Province. Pale pink to white, medium to course grained, even-grained to porphyritic biotite granite to leucogranite, with sparse mafic enclaves; minor biotite leucogranite, aplitic microgranite, aplite.||||||31-MAY-04
14815|Pandora Granite|60425|4|Described|p278-9 Appdx|Early Permian|Late Carboniferous|Of Ootann Suite (Ootann Supersuite).I-type. Fine to med-gr., slightly to mod'ly porphyritic biotite granite to leucogranite; minor slightly altered, slightly porph'ic biotite leucogranite to aplite, and moderately altered, fine-gr., biotite leucogranite||||||07-FEB-11
14851|Papilio Mudstone|23032|5|Briefly described|p28 fig6|Devonian|Devonian|||||||
14851|Papilio Mudstone|41260|4|Described|Table 1|||Reserved as Papilio Creek Mudstone||||||
14851|Papilio Mudstone|41679|2|Defined|p259|Eifelian|late Givetian|||||||
14851|Papilio Mudstone|41719|6|Mentioned|Fig.2|||||||||
14851|Papilio Mudstone|41739|6|Mentioned|Fig.2|||||||||
14851|Papilio Mudstone|41740|6|Mentioned|p222|||||||||
14851|Papilio Mudstone|42031|5|Briefly described|Fig.5 P762|||||||||
14851|Papilio Mudstone|42054|6|Mentioned|p273|||||||||
14851|Papilio Mudstone|42933|3|Fully described|Table 2|||See also p111.||||||
14851|Papilio Mudstone|50093|5|Briefly described|p334|||Of Broken River Group.||||||07-FEB-11
14851|Papilio Mudstone|68298|5|Briefly described|p225|||Nawagiaspis fauna occurrence in a limestone nodule in area mapped as this unit (Withnall et al., 1988, Fig. 80), probably Givetian in age (J.S. Jell, pers. Comm.) but detailed conodont determinations not available.||||||
14851|Papilio Mudstone|68336|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|Includes Spanner Limestone Member.||Calcareous mudstone and minor fine-grained calcareous sandstone and nodular sandstone.|
14851|Papilio Mudstone|68341|5|Briefly described|Map legend.|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|Includes Spanner Limestone Member.||Calcareous mudstone and minor fine-grained calcareous sandstone and nodular sandstone.|
14851|Papilio Mudstone|68478|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|Includes Spanner Limestone Member.|Conformably overlain by the Mytton Formation.|Calcareous mudstone and minor fine-grained calcareous sandstone and nodular sandstone.|
14851|Papilio Mudstone|68479|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|Includes Spanner Limestone Member.|Conformably overlain by the Mytton Formation.|Calcareous mudstone and minor fine-grained calcareous sandstone and nodular sandstone.|
14851|Papilio Mudstone|69592|5|Briefly described|p266|||Southern Graveyard Creek Subprovince, Broken River Province. See also references to Papillio Mudstone (p264) and Papillio Formation (p259). A capping pelitic interval for the Subgroup.||Wandovale Vale Subgroup.||||
14854|Parabarana Sandstone|23394|5|Briefly described|Map legend|Cretaceous|Jurassic|||||||
14854|Parabarana Sandstone|23478|5|Briefly described|p27|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Pelican Well Formation.||||||
14854|Parabarana Sandstone|24176|5|Briefly described|p22 Tb. 1, p19|Early Cretaceous|Early Cretaceous|Kaolinitic sandstone and conglomerate; Aptian flora and fauna.  Geological Province: Mount Painter Province.||||||
14854|Parabarana Sandstone|24392|5|Briefly described|p139, p144 Appendix 1|||Regionally correlative with Cadna-owie Formation (Frakes et al, 1995; Sheard et al, 2000). See also page 140 Fig.1. Geological Province: Eromanga Basin.||||||
14854|Parabarana Sandstone|30176|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|30177|6|Mentioned|p103|||Cretaceous age||||||
14854|Parabarana Sandstone|30807|6|Mentioned|p102|||Suggested map symbol||||||
14854|Parabarana Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
14854|Parabarana Sandstone|33828|6|Mentioned|Table 3|||||||||
14854|Parabarana Sandstone|33939|5|Briefly described|p413|||of the Pelican Well Fm?||||||18-MAR-08
14854|Parabarana Sandstone|34611|4|Described|p153|||Correlation chart. Lower Cretaceous. p152.||||||23-JAN-19
14854|Parabarana Sandstone|36552|6|Mentioned|p59|||||||||
14854|Parabarana Sandstone|36571|6|Mentioned|Table 4|||||||||
14854|Parabarana Sandstone|38007|6|Mentioned|p36|||||||||
14854|Parabarana Sandstone|38068|6|Mentioned|p71|||||||||
14854|Parabarana Sandstone|39211|6|Mentioned|p23|||||||||
14854|Parabarana Sandstone|40926|6|Mentioned|Table 2|||||||||
14854|Parabarana Sandstone|41085|6|Mentioned|Fig.1|||||||||
14854|Parabarana Sandstone|44133|5|Briefly described|p112-113|||||||||
14854|Parabarana Sandstone|46791|6|Mentioned|p42|||||||||
14854|Parabarana Sandstone|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Transitional, non-marine to marine sandstone, siltstone, calcareous sandstone and pebbly sandstone.||||||
14854|Parabarana Sandstone|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone with clasts of quartz, quartzite and porphyry; sand, gravel and shale. U shaped burrows and other fossils.|
14854|Parabarana Sandstone|66303|6|Mentioned|pp27-28.|Early Cretaceous|Early Cretaceous|Stratigraphically equivalent to Cadna-owie Formation.||||||
14854|Parabarana Sandstone|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||||Is overlain unconformably by Bulldog Shale. Is age-equivalent to Cadna-owie Formation in southern Eromanga Basin.||06-FEB-14
14854|Parabarana Sandstone|66623|6|Mentioned|p251.|||Ludbrook (1966). Laterally equivalent to the Cadna-owie Formation.||||||
14854|Parabarana Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Fluvial to marginal marine. Time equivalent to Cadna-owie Formation to the north, and Pelican Well Formation to the west.||Unit in Neales River Group.|Includes Trinity Well Sandstone Member in upper part.|Conformably overlies Murta Formation. Is overlain conformably to unconformably by Bulldog Shale.|Quartz sandstone, gritty to gravelly at base; contains exotic lonestones, occasional pebble lenses and carbonaceous clays as basal channel fill; bioturbated and fossiliferous (bivalves, leaves and wood); upper surface calcite cemented or silcreted.|18-NOV-14
14854|Parabarana Sandstone|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
14854|Parabarana Sandstone|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
14854|Parabarana Sandstone|69019|3|Fully described|p64-65, p85, p87-92, p167.|Cretaceous|Cretaceous|Of Ludbrook (1966); type section ~1 km SE of Parabarana Hill. Composite stratigraphic section in Fig.22. Often associated with ferricrete capping. Fluorite is a pervasive pore filling primary cement, with calcite.||Unit in Neales River Group.||Unconformably overlies Box Bore and Terrapinna Granites. Equivalent to Cadna-owie Formation.|Pale yellowish to pale brown fine-grained quartz sandstone; variably calcite cemented; coarse-grained gritstone lenses; lower zone more silty and dark grey to black from carbonaceous matter; plant fossils abundant.|
14854|Parabarana Sandstone|69023|3|Fully described|p77, p86-88, p93-99, p101, p106, p119|Early Cretaceous|Early Cretaceous|See also p126, p137, p143-144, p151, p159-161, p164, p191-192, p204. Eromanga Basin. Defined by Ludbrook (1966). Type section at Parabarana Hill; detailed profile. Equivalent to Cadna-owie Formation on OODNADATTA map; contrasts between these two units are discussed. Thickness from 3 to ~21m. Tertiary faulting has produced uplift differentials of up to 150m. Overlies Bopeechee Regolith developed on weathered Box Bore and Terrapinna Granites. Is an aquifer, sealed by Bulldog Shale; source for mound springs. Contains calcite and fluorite as pore-filling primary cement. Stratigraphic wells intersection data. Macro-fossils described.|||Includes Trinity Well Sandstone Member.|Unconformably overlies Bopeechee Regolith. Equivalent to Cadna-owie Formation. Is overlain gradationally by Bulldog Shale.|Grey siltstone coarsening upwards to fine- to medium-grained sandstone; sandstone interbeds commonly calcite cemented; a near basal siltstone is commonly carbonaceous; local basal pebbly interval. Local ferricrete capping.|
14854|Parabarana Sandstone|69946|5|Briefly described|p19|||Ludbrook (1966). Crops out on S margin of Eromanga Basin.||||Lateral equivalent of Cadna-owie Formation.||
14854|Parabarana Sandstone|70383|6|Mentioned|p52|||||||Equivalent to Cadna-owie Formation.||
14854|Parabarana Sandstone|70384|5|Briefly described|Map legend.|Aptian|Early Cretaceous|Eromanga Basin. Bioturbated. Fossiliferous: bivalves, leaves, wood. This unit is the rangelands-proximal Basin-wide equivalent to the distal Cadna-owie Formation. Age shown more specifically as Neocomian to Aptian.||of Neales River Group.||Equivalent to Cadna-owie Formation.|Pallid, yellowish, pale grey quartz sandstone, gritty or gravelly at base; exotic lonestones; basal channel infill +/- pebble lenses and trains or carbonaceous clay, local diamictite. Upper 1-2m usually calcite-cemented +/- silcrete +/- ferruginous.|23-JAN-19
14854|Parabarana Sandstone|71342|5|Briefly described|Ch5 p19|||||||Lateral equivalent of the Cadna-owie Formation.||
14854|Parabarana Sandstone|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.  Contains u-shaped burrows and other fossils.|||||Sandstone, calcareous, with clasts of quartz, quartzite and porphyry; sand, gravel and shale.|
14854|Parabarana Sandstone|73251|6|Mentioned|p36|Cretaceous|Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity.||||Unconformably overlain by Bulldog Shale. Equivalent to Cadna-owie Formation.||
14857|Paradise Creek Formation|22438|3|Fully described|p539, Fig.3 p537|Statherian|Statherian|Age of unit 1653+/-7 Ma. See also Fig.10a p546.||||||22-NOV-06
14857|Paradise Creek Formation|22453|6|Mentioned|p 11|||NT and QLD.||||||22-NOV-06
14857|Paradise Creek Formation|22468|5|Briefly described|p 16|Statherian|Statherian|Age: 1653 +/- 7 Ma SHRIMP U/Pb detrital zircons.||||||16-MAR-18
14857|Paradise Creek Formation|22585|6|Mentioned|P739, Fig2, Fig3|||||||||
14857|Paradise Creek Formation|22665|6|Mentioned|P221, Table1||Statherian|Age of unit is 1653+/-7 Ma.||||||22-NOV-06
14857|Paradise Creek Formation|22680|6|Mentioned|84|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|22747|6|Mentioned|Table1,p7|||With Gunpowder Creek Formation correlates with Suprise Creek Beds and Ploughed Mountain Beds||||||
14857|Paradise Creek Formation|23031|5|Briefly described|53|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain byEsperanza Formation; underlain by Gunpowder Creek Formation||||||22-NOV-06
14857|Paradise Creek Formation|23073|5|Briefly described|p744 (Fig 2), p745|||||||||
14857|Paradise Creek Formation|23198|6|Mentioned|p873|||||||||
14857|Paradise Creek Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
14857|Paradise Creek Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Includes the Mount Oxide Chert Member.  Of McNamara Group.||||||07-NOV-08
14857|Paradise Creek Formation|23396|4|Described|p420|Statherian|Statherian|Of the McNamara Group.  Age: 1658+/-3Ma.||||||22-NOV-06
14857|Paradise Creek Formation|23397|5|Briefly described|p469|Statherian|Statherian|||||||
14857|Paradise Creek Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group.  Age: 1659-1653Ma.||||||22-NOV-06
14857|Paradise Creek Formation|23399|5|Briefly described|p493 Fig.3|||Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|23405|5|Briefly described|p589|||||||||
14857|Paradise Creek Formation|23406|5|Briefly described|p611|||Geological province: Lawn Hill Platform. Includes deep to shallow marine carbonates.||||||16-JUN-09
14857|Paradise Creek Formation|23407|5|Briefly described|p632|||||||||
14857|Paradise Creek Formation|23408|4|Described|p512|||Of the McNamara Group. Contains numerous reworked tuffaceous beds, which may correlate with upper Mount Isa Group; and also, rhythmically laminated distal tempestite facies, dolomudstone and dolosiltstone.||||||30-MAY-14
14857|Paradise Creek Formation|23409|5|Briefly described|p535 Fig.2|||Of the McNamara Group||||||22-NOV-06
14857|Paradise Creek Formation|23466|5|Briefly described|p267|||||||||
14857|Paradise Creek Formation|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
14857|Paradise Creek Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
14857|Paradise Creek Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 500m.||||||
14857|Paradise Creek Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
14857|Paradise Creek Formation|23986|5|Briefly described|p65|Proterozoic|Proterozoic|Of McNamara Group.||||||
14857|Paradise Creek Formation|24033|6|Mentioned|p25|||||||||
14857|Paradise Creek Formation|24156|5|Briefly described|p18, p19, p22|||Forms plateaux, rises and pediments with lateritic duricrust, mottled zone and ferruginous saprolite.|||||Dolomitic siltstone, minor sandstone and chert.|
14857|Paradise Creek Formation|24308|5|Briefly described|p1002, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin.||||||07-NOV-08
14857|Paradise Creek Formation|24309|5|Briefly described|p1018|Proterozoic|Proterozoic|Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|24419|6|Mentioned|p18|||Includes Mount Oxide Chert Member.||||||09-MAR-05
14857|Paradise Creek Formation|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlain by Esperanza Formation. Age: c. 1658 Ma. Geological Province: Lawn Hill Platform.||||||
14857|Paradise Creek Formation|29969|5|Briefly described|p392|||||||||
14857|Paradise Creek Formation|30354|6|Mentioned|p9|||Refers to micropalaeontology.||||||
14857|Paradise Creek Formation|30535|6|Mentioned|p404|||Refers de Keyser(1958)||||||
14857|Paradise Creek Formation|30778|6|Mentioned|Fig.3|||||||||
14857|Paradise Creek Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14857|Paradise Creek Formation|31207|6|Mentioned|p1414|||||||||
14857|Paradise Creek Formation|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
14857|Paradise Creek Formation|31396|6|Mentioned|p1188|||||||||
14857|Paradise Creek Formation|31704|6|Mentioned|p4|||Favourable horizon for copper||||||
14857|Paradise Creek Formation|31821|5|Briefly described|p1024|||||||||
14857|Paradise Creek Formation|31877|5|Briefly described|p378|||||||||
14857|Paradise Creek Formation|32264|5|Briefly described|p383|||||||||
14857|Paradise Creek Formation|32287|6|Mentioned|Fig. 1|||||||||
14857|Paradise Creek Formation|32478|6|Mentioned|p223|||||||||
14857|Paradise Creek Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|32660|5|Briefly described|Table 5|||||||||
14857|Paradise Creek Formation|32722|6|Mentioned|Fig.2|||Carpentarian. Stromatolite||||||
14857|Paradise Creek Formation|32959|6|Mentioned|Fig.21|||||||||
14857|Paradise Creek Formation|33111|6|Mentioned|p28|||||||||
14857|Paradise Creek Formation|33900|5|Briefly described|p15|||||||||
14857|Paradise Creek Formation|34395|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
14857|Paradise Creek Formation|34754|6|Mentioned|p42|||||||||
14857|Paradise Creek Formation|34891|6|Mentioned|p240|||||||||
14857|Paradise Creek Formation|35001|6|Mentioned|Fig.45|||||||||
14857|Paradise Creek Formation|35004|6|Mentioned|p266|||||||||
14857|Paradise Creek Formation|35032|6|Mentioned|p117|||||||||
14857|Paradise Creek Formation|35074|6|Mentioned|Fig.2|||||||||
14857|Paradise Creek Formation|35115|6|Mentioned|p207|||||||||
14857|Paradise Creek Formation|35261|6|Mentioned|p338|||||||||
14857|Paradise Creek Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|36715|6|Mentioned|p13|||||||||
14857|Paradise Creek Formation|37371|6|Mentioned|p368|||||||||
14857|Paradise Creek Formation|37459|1|Redefined|p428|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
14857|Paradise Creek Formation|37555|6|Mentioned|p2|||||||||
14857|Paradise Creek Formation|37569|5|Briefly described|p91|||||||||
14857|Paradise Creek Formation|37572|6|Mentioned|Fig.7|||||||||
14857|Paradise Creek Formation|38232|6|Mentioned|p89|||||||||
14857|Paradise Creek Formation|38237|4|Described|p128|||||||||
14857|Paradise Creek Formation|38243|6|Mentioned|p354|||||||||
14857|Paradise Creek Formation|38276|6|Mentioned|Fig.1|||||||||
14857|Paradise Creek Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|38348|4|Described|p10|||||||||
14857|Paradise Creek Formation|38444|5|Briefly described|p105|||||||||
14857|Paradise Creek Formation|38446|4|Described|p186|||||||||
14857|Paradise Creek Formation|38584|6|Mentioned|p22|||||||||
14857|Paradise Creek Formation|39125|6|Mentioned|p163|||||||||
14857|Paradise Creek Formation|39210|6|Mentioned|Table 3|||||||||
14857|Paradise Creek Formation|39445|5|Briefly described|Table 2|||See also p41.||||||22-NOV-06
14857|Paradise Creek Formation|39492|6|Mentioned|p31|||||||||
14857|Paradise Creek Formation|39497|6|Mentioned|Fig.4|||||||||
14857|Paradise Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of McNamara Gp. Includes Mount Oxide Chert Member at base. Stromatolitic dolomite, dolomitic siltstone, some some limestone interbeds, dolomite with chert nodules after.... Overlain by Esperanza Formation; overlies Gunpowder Creek Fm.||||||15-JUN-06
14857|Paradise Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|39925|6|Mentioned|Fig.9|||||||||
14857|Paradise Creek Formation|39943|6|Mentioned|Table 1A|||||||||
14857|Paradise Creek Formation|39944|3|Fully described|p238|||||||||
14857|Paradise Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
14857|Paradise Creek Formation|40221|3|Fully described|p15|||||||||
14857|Paradise Creek Formation|40394|6|Mentioned|p285|||||||||
14857|Paradise Creek Formation|40623|5|Briefly described|p96|||||||||
14857|Paradise Creek Formation|40858|6|Mentioned|p136|||||||||
14857|Paradise Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
14857|Paradise Creek Formation|41862|6|Mentioned|p474|||||||||
14857|Paradise Creek Formation|42166|6|Mentioned|p108|||||||||
14857|Paradise Creek Formation|43235|5|Briefly described|p9,Fig.10.|||Of the McNamara Group.||||||22-NOV-06
14857|Paradise Creek Formation|44091|14|Not recorded|p10||Mesoproterozoic|||||||
14857|Paradise Creek Formation|44115|14|Not recorded|p17|||||||||
14857|Paradise Creek Formation|44210|2|Defined|Tb.1,p9,map|||||||||
14857|Paradise Creek Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
14857|Paradise Creek Formation|44216|14|Not recorded|p385|||Dolomite and dolomitic sandstone.||||||
14857|Paradise Creek Formation|44271|2|Defined|p35,36,41|||Overlies Gunpowder Creek Formation.||||||
14857|Paradise Creek Formation|44275|14|Not recorded|Map Legend|||||||||
14857|Paradise Creek Formation|44279|14|Not recorded|Tb.1|||||||||
14857|Paradise Creek Formation|44290|2|Defined|p438,439|||Precambrian probably Palaeoproterozoic.||||||
14857|Paradise Creek Formation|44521|14|Not recorded|p8,21,map|||upper Early Proterozoic.||||||
14857|Paradise Creek Formation|44526|14|Not recorded|p253|||Probably contemporaneous in part with Mount Isa Shale.||||||
14857|Paradise Creek Formation|44552|14|Not recorded|p9|||||||||
14857|Paradise Creek Formation|44587|14|Not recorded|p381|||Affected by laterisation.||||||
14857|Paradise Creek Formation|44751|14|Not recorded|p302|||Dolomitic, with numerous stromatolites. A little younger than the 1st main deformation of the area.||||||
14857|Paradise Creek Formation|44788|14|Not recorded|p9|||||||||
14857|Paradise Creek Formation|44989|2|Defined|p.35,39,42,53-255|||Tb.II,III. On many pages. (E54-13,F54-1). Pl.15,22.||||||
14857|Paradise Creek Formation|45287|14|Not recorded|p.225,226||Paleoproterozoic|||||||07-NOV-08
14857|Paradise Creek Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
14857|Paradise Creek Formation|47083|3|Fully described|p15-16||Proterozoic|Equivalent to Paradise Fm of Cavaney (1975). Of McNamara Gp. Overlain by Esperanza Fm; underlain by Gunpowder Creek Fm. Max. thickness 750 m.||||||22-NOV-06
14857|Paradise Creek Formation|50332|6|Mentioned|p21|Proterozoic|Proterozoic|Includes the Mount Oxide Chert Member.||||||07-FEB-11
14857|Paradise Creek Formation|50550|5|Briefly described|p1139 Fig.2, p1143 Fig.6||Statherian|Age: 1659 Ma, 1657Ma. Overlies Mount Oxide Chert conformably. Conformably overlain by Esperanza Formation. Geological Province: Western Fold Belt.||||||19-DEC-07
14857|Paradise Creek Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Laminated dolomite and silicified siltstone.  Overlies Gunpowder Creek Formation; overlain by Esperanza Formation.||||||28-JUN-04
14857|Paradise Creek Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Esperanza Formation, underlain by Gunpowder Creek Formation.||||||
14857|Paradise Creek Formation|61732|5|Briefly described|p25|||Superseded by Esperanza Formation.  Contains microfossils in stromatolites. In the Mount Isa region.||||||07-FEB-11
14857|Paradise Creek Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
14857|Paradise Creek Formation|62084|4|Described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Paradise Ck Fm.|1658+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Platform carbonates.|
14857|Paradise Creek Formation|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Two other similar ages are given.|1654 +/- 4 Ma.|McNamara Group.||||
14857|Paradise Creek Formation|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: ca 1660-1655Ma. Of the Gun Supersequence.||||||07-NOV-08
14857|Paradise Creek Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
14857|Paradise Creek Formation|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sanstone and siltstones, dolomudstones, laminated carbonates.||||||07-FEB-11
14857|Paradise Creek Formation|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Gun supersequence. Appears in Fig.2 only as Par. Ck.|c.1657 Ma.|Of the McNamara Group||||
14857|Paradise Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||||||
14857|Paradise Creek Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
14857|Paradise Creek Formation|63116|6|Mentioned|p1297 Fig.2, p1299 Tb.1, p1300 |||Isa superbasin. Material properties detailed.||||||
14857|Paradise Creek Formation|63866|5|Briefly described|p57-p58|Statherian|Statherian|Isa Superbasin.|1657 +/- 3 Ma (Page et al., 2000)|Gun Supersequence||||
14857|Paradise Creek Formation|63884|5|Briefly described|p14|||Mainly dolomitic. In contact with Gunpowder Creek Formation. Equivalent to Urquhart Shale.||||||
14857|Paradise Creek Formation|64250|6|Mentioned|p11 fig 3||||1658 +/- 3 Ma - 1653 +/- 7 Ma.|Unit in McNamara Group.||||
14857|Paradise Creek Formation|64575|6|Mentioned|p665|||||||||
14857|Paradise Creek Formation|65337|6|Mentioned|p30, p33.||||> c.1654 Ma.|||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.||
14857|Paradise Creek Formation|65396|5|Briefly described|p82, p175, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform. Detrital zircon sources listed.|1654 +/- 3 Ma|McNamara Group||Overlies Upper Gunpowder Creek Formation; overlain by Esperanza Formation.||04-APR-17
14857|Paradise Creek Formation|66844|5|Briefly described|p243-244,251-254, 267-268,271,273|||Lawn Hill Platform. SHRIMP zircon ages of 1653+\-7, 1654+\-3, 1658+\-3 and 1659+\-3 Ma. Lower part coincides with decline in accommodation rates and reduction of siliciclastic influx, leading to carbonate facies deposition from Gun 1.5. Stromatolites, present at specific horizons, are dominantly domal-columnar, indicative of shallow sub-tidal and peritidal environments.||Of lower McNamara Group; Within Gun supersequences.|Informally subdivided into upper and lower parts.||Includes quartz peloid grainstone; intraclast grainstone; quartz arenite-intraclast grainstone; microbial laminite; domal stromatolites with quartz peloid grainstone and dolomudstone.|
14857|Paradise Creek Formation|67323|5|Briefly described|GIS attrib tbl,  p26, p34, p60|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.|1659 +/- 3 Ma to 1653 +/- 7 Ma.|Of McNamara Group.|||Stromatolitic dolomite, dolomitic siltstone, some limestone interbeds, dolomite with chert nodules after anhydrite; minor pink to grey fine tuff.|
14857|Paradise Creek Formation|68020|6|Mentioned|p125|||Includes Lady Annie and Mount Kelly group of Cu +/- Au deposits.||||Correlated with lower Mount Isa Group.||
14857|Paradise Creek Formation|68542|5|Briefly described|p6|||||Lower McNamara Group||Overlain by Esperanza Formation, overlies Gunpowder Creek Formation|Dolomitic siltstone and sandstone.|
14857|Paradise Creek Formation|68576|5|Briefly described|Q_2: p6-7|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.|Dolomitic siltstone and sandstone.|
14857|Paradise Creek Formation|68732|6|Mentioned|p162, p163, p165 Fig.3, p168 Fig.5, p169|Statherian|Statherian|Of the Gun Supersequence. Ages for pinkites in this formation range from 1658 +/- 3 Ma to 1654 +/- 3 Ma. Sedimentary depositional ages.|1658 +/- 3, 1653 +/- 7, 1654 +/- 4, 1657 +/- 3 Ma|Of the McNamara Group.|||Contains stromatolitic bioherms and biostromes.|01-DEC-17
14857|Paradise Creek Formation|69591|4|Described|p42-45, p54, p88|||Isa Superbasin. Deposited on a shallow carbonate platform: deep marine/tempestites to peritidal deposits. Contains Conophytons. Part of Gun Supersequence.|1657 +/- 3 Ma (MDA: Page et al., 2000).|McNamara Group.||Overlies Gunpowder Creek Formation. Is overlain by Esperanza Formation.|Stromatolitic dolomite, dolomitic siltstone, some limestone interbeds, dolomite with chert nodules after anhydrite; minor pink to grey fine tuff.|
14857|Paradise Creek Formation|70864|5|Briefly described|p75, 74 Fig 2, p77, 78, 80,81,82,84,100|Mesoproterozoic||Breccia hosted Fe and Cu Sulphide mineralization.||McNamara Group|||Stromatolitic dolostone, dolomitic and carbonaceous siltstone, chert and sandstones.|
14857|Paradise Creek Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1653+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
14857|Paradise Creek Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. 4 sedimentary depositional ages listed for this unit. Oldest and youngest listed in age field.|1658 +/- 3 Ma to 1653 +/- 7 Ma|McNamara Group||Overlies upper Gunpowder Formation and underlies Esperanza Formation.||
14857|Paradise Creek Formation|72527|6|Mentioned|p91, p105.|Statherian|Statherian|In Lawn Hill 1:250 K sheet area. Depositional age suggested as being simliar to Drummond Formation.|1658-1653 Ma (Page et al., 2000)|McNamara Group||Suggested to be laterally equivalent with Brumby and Drummond Formation.||
14857|Paradise Creek Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Four U-Pb zircon sedimentary depositional ages given for this unit on p5 are shown for the overlying Esperanza Formation on p33.|1658 +/- 3 Ma to 1653 +/- 7 Ma|McNamara Group||Overlies Gunpowder Creek Formation and underlies Esperanza Formation.|Includes dolostone.|
14857|Paradise Creek Formation|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.||McNamara Group||Overlies Gunpowder Creek Formation and underlies Esperanza Formation.|Includes dolostone.|
14857|Paradise Creek Formation|72919|6|Mentioned|p56, p63|||Mount Isa Province. Tuff crystallisation age of ca. 1658 Ma reported by Page et al. (2000).||||||
14857|Paradise Creek Formation|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1657+/-3, 1654+/-3, 1653+/-7, 1658+/-3 Ma|McNamara Group||Underlain by Gunpowder Formation. Overlain by Esperanza Formation.||
14857|Paradise Creek Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Gun Supersequence. Partial aquifer.||McNamara Group||Underlain by Gunpowder Creek Formation. Overlain by Esperanza Formation.||
14857|Paradise Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1658+/-3 Ma, 1657+/-3 Ma, 1653+/-7 Ma||||Carbonates.|
14921|Pascoe River beds|22811|3|Fully described|p603|Carboniferous|Devonian|||||||
14921|Pascoe River beds|23420|5|Briefly described|p 129, 372|Early Carboniferous|Late Devonian|Pascoe River Basin||||||21-DEC-11
14921|Pascoe River beds|23430|5|Briefly described|p510|||Pascoe River Basin Province.||||||
14921|Pascoe River beds|42550|4|Described|p8|||||||||
14921|Pascoe River beds|42637|5|Briefly described|p8|||||||||
14921|Pascoe River beds|44081|14|Not recorded|p216|||||||||
14921|Pascoe River beds|49769|6|Mentioned|p4|||||||||
14921|Pascoe River beds|69591|5|Briefly described|p74 Fig.2.71, p101|Carboniferous|Late Devonian|Pascoe River Basin; Coen Inlier, Etheridge Province. Crops out along several (named) creeks and on Haggarstone Island. Up to ~600m thick; average is ~200m. Fluvial, flood-plain and lacustrine deposits.||||Is overlain by Janet Ranges Volcanics. Is intruded by Weymouth Granite.|A folded and faulted succession of carbonaceous siltstone, shale, tuff and variably tuffaceous sandstone with thin beds of coal.|
14921|Pascoe River beds|70207|6|Mentioned|p126|Carboniferous|Carboniferous|||||||
14921|Pascoe River beds|71853|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian||||||Sandstone, arkose, siltstone, shale, tuff, coal, conglomerate, minor chert.|
14921|Pascoe River beds|72297|5|Briefly described|p694|Early Carboniferous|Early Carboniferous|Coen Inlier, Cape York Peninsula. Oldest-known coal-bearing strata in QLD. Forms a wedge of steeply-tilted and highly fractured down-faulted blocks. Unlikely to be commercially significant.|||||Includes several stony coal seams, generally <1.8m thick.|
14921|Pascoe River beds|72983|6|Mentioned|p66|early Carboniferous|early Carboniferous|||||Overlain by Janet Ranges Volcanic Group.||
14936|Patchawarra Formation|13497|4|Described|iv, v, vi, viii, ix, x|Artinskian|Asselian|Cooper Basin.  Named for the Patchawarra Bore by Kapel (1972). Petrography and lithology described in detail. A sedimentary facies log is provided. The lower part of this formation is lithologically similar to the Tirrawarra Sandstone.  Up to 680m thick in the Nappamerri Trough. Coal and carbonaceous shale of this unit are the primary source rocks of the Cooper Basin. Total thickness up to 373.4m. Hosts large gas reservoirs and is sealed by Murteree Shale. Informally referred to a as  "lower" and "upper" subunits. See also  xi, xii, p55, p61, p63-p64, p69 fig 6.1, p70-p73, p75, p86-p94, p99, p119, p122, p124-p127, p129, p131, p132 tbl 8.1, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p154, p157, p159-p161, p168-p172, p174-p176, p182-p184, p190-p196, p204-p205, p208, p216.||Gidgealpa Group|Includes the Malabine Coal.|Overlies and interfingers with the Tirrawarra Sandstone. Overlies the Merrimelia Formation. Conformably overlain by the Murteree Shale. Disconformably overlain by the Toolachee Formation.|Interbedded fine to medium-grained, locally coarse-grained and pebbly sandstone, grey to black siltstone, shale and coal.|
14936|Patchawarra Formation|13516|6|Mentioned|p147 fig 5, p148|Early Permian|Early Permian|From Cooper Basin. Loosely correlated with top of the Reids Dome beds and basal Cattle Creek Formation.||||||
14936|Patchawarra Formation|22527|5|Briefly described|p 1, 2, 3, Fig1, 3|||||||||
14936|Patchawarra Formation|22839|6|Mentioned|P33|||||||||
14936|Patchawarra Formation|22883|6|Mentioned|P29|||||||||
14936|Patchawarra Formation|22924|6|Mentioned|49|||||||||
14936|Patchawarra Formation|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Cooper Basin.  Of the Gidgealpa Group.||||||22-NOV-06
14936|Patchawarra Formation|23155|4|Described|p17|Early Permian|Early Permian|Unit up to 450m thick.  Spore pollen assemblages are Asselian - Kungurian in age.||||||
14936|Patchawarra Formation|23356|5|Briefly described|26 Tab.2|Early Permian|Early Permian|||||||
14936|Patchawarra Formation|23359|5|Briefly described|73|Early Permian|Early Permian|||||||
14936|Patchawarra Formation|23375|4|Described|Fig2 p265,285|Artinskian|Sakmarian|In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|23832|4|Described|p328|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24199|5|Briefly described|p512|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24204|5|Briefly described|p284|Permian|Permian|Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Tirrawarra and Merrimelia Formations.  Geological Province: Cooper Basin.  See also p132.||||||22-NOV-06
14936|Patchawarra Formation|24212|4|Described|p65,  p67 Fig. 3p|Early Permian|Early Permian|Age: 280Ma.  Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|24620|6|Mentioned|p6|||Referred to in text as Patchawarra only - intended to be Patchawarra Formation.  Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|29387|6|Mentioned|Table 2|||Refs to Gatehouse(1972).||||||
14936|Patchawarra Formation|29389|6|Mentioned|p18|||Permian.||||||
14936|Patchawarra Formation|29391|6|Mentioned|Table 5|||See p23.||||||22-NOV-06
14936|Patchawarra Formation|29513|6|Mentioned|p23|||||||||
14936|Patchawarra Formation|29515|6|Mentioned|p14|||||||||
14936|Patchawarra Formation|29518|6|Mentioned|p24|||||||||
14936|Patchawarra Formation|29721|6|Mentioned|p182|||||||||
14936|Patchawarra Formation|29729|6|Mentioned|p266|||||||||
14936|Patchawarra Formation|30519|5|Briefly described|p73|||See also p75. Part of Gidgealpa Group.||||||22-NOV-06
14936|Patchawarra Formation|30540|6|Mentioned|p65|||General Geology||||||
14936|Patchawarra Formation|30542|6|Mentioned|p50|||||||||
14936|Patchawarra Formation|30544|6|Mentioned|p52|||||||||
14936|Patchawarra Formation|30825|6|Mentioned|p37|||||||||
14936|Patchawarra Formation|30873|3|Fully described|p14|||||||||
14936|Patchawarra Formation|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Age is Sakamarian - Artinskian.||||||22-NOV-06
14936|Patchawarra Formation|31591|3|Fully described|p54|||See also p55, 56, 57. Early to Lower Permian.||||||05-OCT-06
14936|Patchawarra Formation|32696|6|Mentioned|Fig.4|||See also Figs. 6,7,8,9||||||
14936|Patchawarra Formation|33074|6|Mentioned|p260|||||||||
14936|Patchawarra Formation|33331|6|Mentioned|p38|||||||||
14936|Patchawarra Formation|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) and Gatehouse (1972)||||||22-NOV-06
14936|Patchawarra Formation|33523|6|Mentioned|p26|||||||||
14936|Patchawarra Formation|33971|6|Mentioned|p33|||||||||
14936|Patchawarra Formation|33976|6|Mentioned|p9|||Similar to Purni Formation.||||||22-NOV-06
14936|Patchawarra Formation|34839|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|35067|6|Mentioned|Fig.4|||||||||
14936|Patchawarra Formation|35068|6|Mentioned|Fig.3|||Discussed p54.||||||22-NOV-06
14936|Patchawarra Formation|35151|6|Mentioned|p147|||||||||
14936|Patchawarra Formation|35279|6|Mentioned|p19|||||||||
14936|Patchawarra Formation|35457|6|Mentioned|p627|||Also Fig.4 biostratigraphic relationships||||||
14936|Patchawarra Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
14936|Patchawarra Formation|35845|4|Described|p24|||Lithology and depositional environments. See also Fig.25||||||05-OCT-06
14936|Patchawarra Formation|36099|6|Mentioned|p191|||||||||
14936|Patchawarra Formation|36172|6|Mentioned|Appendix|||||||||
14936|Patchawarra Formation|36613|6|Mentioned|p1864|||||||||
14936|Patchawarra Formation|36910|6|Mentioned|p60|||||||||
14936|Patchawarra Formation|36917|6|Mentioned|Fig.1|||||||||
14936|Patchawarra Formation|36924|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|37065|6|Mentioned|p30|||||||||
14936|Patchawarra Formation|37103|5|Briefly described|p266|||||||||
14936|Patchawarra Formation|37287|6|Mentioned|p36|||||||||
14936|Patchawarra Formation|37703|6|Mentioned|p2240|||||||||
14936|Patchawarra Formation|37855|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|37917|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|38958|5|Briefly described|p491|||||||||
14936|Patchawarra Formation|38977|6|Mentioned|Fig.1|||||||||
14936|Patchawarra Formation|39252|5|Briefly described|p20|||See also p13 and p22.||||||22-NOV-06
14936|Patchawarra Formation|39254|5|Briefly described|p46|||See also p47.||||||22-NOV-06
14936|Patchawarra Formation|39255|6|Mentioned|p51|||||||||
14936|Patchawarra Formation|39261|6|Mentioned|Fig. 9|||||||||
14936|Patchawarra Formation|39264|6|Mentioned|Fig. 13|||||||||
14936|Patchawarra Formation|39265|6|Mentioned|Fig. 3|||||||||
14936|Patchawarra Formation|39276|6|Mentioned|Fig. 2|||||||||
14936|Patchawarra Formation|39445|5|Briefly described|Table 8|||See also p94.||||||22-NOV-06
14936|Patchawarra Formation|39478|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|39494|6|Mentioned|Fig.3|||||||||
14936|Patchawarra Formation|39757|6|Mentioned|p1601|||||||||
14936|Patchawarra Formation|40030|6|Mentioned|p131|||See also Fig.3||||||
14936|Patchawarra Formation|40249|6|Mentioned|p45|||||||||
14936|Patchawarra Formation|40544|6|Mentioned|p157|||||||||
14936|Patchawarra Formation|40637|6|Mentioned|Fig.2|||||||||
14936|Patchawarra Formation|41060|6|Mentioned|Fig.5|||||||||
14936|Patchawarra Formation|41099|6|Mentioned|p185|||||||||
14936|Patchawarra Formation|41123|6|Mentioned|p180|||||||||
14936|Patchawarra Formation|41131|5|Briefly described|Table 1|||||||||
14936|Patchawarra Formation|41164|6|Mentioned|p422|||||||||
14936|Patchawarra Formation|41165|6|Mentioned|Fig.18|||||||||
14936|Patchawarra Formation|41166|6|Mentioned|p379|||||||||
14936|Patchawarra Formation|41183|6|Mentioned|Fig.3 p308|||||||||
14936|Patchawarra Formation|41184|6|Mentioned|p346|||||||||
14936|Patchawarra Formation|41189|6|Mentioned|p249|||||||||
14936|Patchawarra Formation|41198|6|Mentioned|p44|||||||||
14936|Patchawarra Formation|41214|6|Mentioned|p256|||||||||
14936|Patchawarra Formation|41221|6|Mentioned|p392|||||||||
14936|Patchawarra Formation|41226|6|Mentioned|p22|||||||||
14936|Patchawarra Formation|41247|6|Mentioned|p117|||||||||
14936|Patchawarra Formation|41267|6|Mentioned|p256|||||||||
14936|Patchawarra Formation|41288|6|Mentioned|p156|||||||||
14936|Patchawarra Formation|41491|6|Mentioned|p180|||||||||
14936|Patchawarra Formation|41595|5|Briefly described|p30|||||||||
14936|Patchawarra Formation|41689|6|Mentioned|Table 1|||||||||
14936|Patchawarra Formation|41707|6|Mentioned|Fig.8|||||||||
14936|Patchawarra Formation|41712|6|Mentioned|p282|||||||||
14936|Patchawarra Formation|41720|6|Mentioned|p370|||||||||
14936|Patchawarra Formation|42064|6|Mentioned|Fig.5 P.171|||||||||
14936|Patchawarra Formation|42085|6|Mentioned|Fig.2 P374|||||||||
14936|Patchawarra Formation|42150|6|Mentioned|p65|||||||||
14936|Patchawarra Formation|42153|6|Mentioned|p361|||||||||
14936|Patchawarra Formation|42154|6|Mentioned|p361|||||||||
14936|Patchawarra Formation|42187|6|Mentioned|Fig.3 P318|||||||||
14936|Patchawarra Formation|42256|6|Mentioned|Fig.1 P243|||||||||
14936|Patchawarra Formation|42395|6|Mentioned|p80|||||||||
14936|Patchawarra Formation|42496|5|Briefly described|App.1 P152, Fig.3 P2|||||||||
14936|Patchawarra Formation|42547|5|Briefly described|p81|||||||||
14936|Patchawarra Formation|42599|6|Mentioned|p624|||In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|42648|5|Briefly described|p41, p48|||||||||
14936|Patchawarra Formation|42746|5|Briefly described|p6|||In the Cooper Basin.||||||22-NOV-06
14936|Patchawarra Formation|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
14936|Patchawarra Formation|43018|5|Briefly described|Table 1,p386|||||||||
14936|Patchawarra Formation|43105|5|Briefly described|p14|||||||||
14936|Patchawarra Formation|43570|4|Described|p533,Fig.2,p535,|Sakmarian|Asselian|p541-4, p550-552.||||||05-OCT-06
14936|Patchawarra Formation|43628|6|Mentioned|Fig.3||Early Permian|||||||
14936|Patchawarra Formation|43711|6|Mentioned|p19|||||||||
14936|Patchawarra Formation|44133|4|Described|p65 Fig. 8.4, 84|Permain|Permain|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlies Tirrawarra Sandstone. Maximum Thickness: 680m. Conformably underlies the Murteree Shale.||||||22-NOV-06
14936|Patchawarra Formation|46849|6|Mentioned|Fig. 7|||||||||
14936|Patchawarra Formation|48995|6|Mentioned|Fig.3|||||||||
14936|Patchawarra Formation|60386|6|Mentioned|p296|Artinskian|Sakmarian|Cooper Basin. Non-marine, coal.||||||
14936|Patchawarra Formation|60717|5|Briefly described|p40, p41|Artinskian|Asselian|Of the Gidgealpa Group. Overlain by Murteree Shale; overlies Tirrawarra Sandstone. Thickness: 680m. Geological Province: Cooper Basin. See also Figure 2.||||||31-JAN-08
14936|Patchawarra Formation|61015|6|Mentioned|p46|||||||||
14936|Patchawarra Formation|61250|6|Mentioned|p45|||Contains petroleum systems. Geological Province: Cooper Basin.||||||18-AUG-05
14936|Patchawarra Formation|61614|5|Briefly described|p289, p290, p292, p295, p290 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin. Contain coal and shale lithologies.||||||17-MAR-09
14936|Patchawarra Formation|61616|6|Mentioned|p329, p330, p331, p338, p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|61617|6|Mentioned|p343, p344, p346, p346 Tb. 3|Permian|Permian|Net coal thickness: 40-60m. Geological Province: Cooper Basin.||||||
14936|Patchawarra Formation|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|62730|5|Briefly described|p352 Fig. 1|Late permian|Early Permian|Geological Province: Cooper Basin.||||||21-APR-08
14936|Patchawarra Formation|62759|5|Briefly described|p1|||Geological Province: Cooper Basin.||||||05-FEB-08
14936|Patchawarra Formation|63978|2|Defined|p11, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Gp.Conformable on Tirrawarra Sst.or unconformable on Merrimelia Fm; conformable below Murteree Shale. In northern Cooper Basin - overlain by Toolachee Formation. Upwardly fining sst.,siltstone, mudstone and coal...detailed lith. included||||||09-APR-13
14936|Patchawarra Formation|64048|5|Briefly described|p63, p64 Tb. 2, p65-66|Permian|Permian|Unconformably overlain by Toolachee Formation where the Murteree and Epsilon Formations, and Roseneath Shale are absent. Source of hydrocarbons - coal measures. Geological Province: Cooper Basin.||||||07-FEB-11
14936|Patchawarra Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Middle Permian|Middle Permian|Cooper Basin.||||Underlies the Murteree Shale and Roseneath Shale. Overlies the Tirrawarra Sandstone and Merrimelia Formation.||11-DEC-15
14936|Patchawarra Formation|64232|5|Briefly described|p12|||Geological Province: Cooper Basin/ Weena Trough. Shallow occurrences of thick sub-bituminous coal seams are present in this unit.||||||24-JUL-08
14936|Patchawarra Formation|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hosts coal: equivalent to Aramac Coal Measures (Galilee Basin) and Reids Dome beds and Collinsville Coal Measures (Bowen Basin). Contains hydrocarbon source rocks and reservoirs; also thought to have charged the underlying Merrimelia Formation and Tirrawarra Sandstone reservoirs.||||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|65489|5|Briefly described|p11, p15-16, p45-49, p55, p73, p91, p96|Artinskian|Asselian|See also p132, p143, p158. Cooper Basin. Major source unit. Gas flow was announced from this unit by Bridge Oil in 1970. Gas and oil reservoir accounting for 32% and 5% respectively of the Basin's production.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone and Merrimelia Formation. Is overlain by Murteree Shale. Is correlated with Purni Formation (Pedirka Basin).|Includes abundant coals and multi-zone high-sinuosity fluvial sandstones.|
14936|Patchawarra Formation|65925|5|Briefly described|Appendix 2.||||||||Siltstone, coal-swamp; sandstone; minor coal. Fluviolacustrine floodplain, minor deltaic environments.|
14936|Patchawarra Formation|67402|5|Briefly described|p90 fig CPR4, p91 tbl CPR1|||Cooper Basin. Prospective reservoir for the storage of carbon dioxide with a potential storage capacity of 3.4 Megatonnes. Deposited in low to moderate energy fluvial environments dominated by highly meandering rivers and their floodplains. Up to 400m thick. See also p90-p94, p98, p99 fig CPR14, p100, p101, p101 tbl CPR2, p104, p105, p268.||Gidgealpa Group||Overlain by the Murteree Shale and Toolachee Formation. Overlies the Tirrawarra Sandstone.|Fining upwards deposits of fine to medium-grained sandstone, siltstone, shale and major coal beds.|
14936|Patchawarra Formation|68068|5|Briefly described|Map legend|Early Permian|Early Permian|Cooper Basin (subsurface only). Stacked channel and upward-fining deposits. Fluvial (point bars, meandering river), backswamp and floodbasin environments. Spore-pollen assemblage is of cold to cool-temperate flora.||Unit in Gidgealpa Group.||Conformably overlies Tirrawarra Formation. Is conformably overlain by Murteree Shale.|Interbedded, grey, buff or brown sandstone (locally pebbly), mudstone with carbonaceous partings and coal; thick coal seams in lower part; upper levels dominated by mudstone with thin interbeds of siltstone and sandstone.|
14936|Patchawarra Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p206, p207|Cisuralian|Cisuralian|Kapel (1972); Gatehouse (1972). ~ 50 to > 500 m thick. Palynofloras are Cisuralian (Gray and McKellar 2002). Authigenic quartz, kaolinite and dicktite are common in sandstones. Coal seams are up to 16m thick. Interdigitates with the Murteree Shale.||Of the Gidgealpa Group.||Underlain/unconformably underlain by the Tirrawarra Sandstone and the Merrimelia Formation respectively. Conformably overlain by the Murteree Shale. Unconformably overlain by the Toolachee Formation.|Comprises a very widespread, upward fining, interbedded sandstone, siltstone, mudstone and coal succession.|17-JUL-14
14936|Patchawarra Formation|69019|6|Mentioned|p146.|Permian|Permian|Partial erosion of lower levels and evidence of stream rejuvenation in middle levels suggest structural movements in the Cooper Basin in the Early Permian.||||||
14936|Patchawarra Formation|69023|3|Fully described|p79, p81, p82 Fig.18, p83-85, p150|Permian|Permian|See also p163, p191-192. Cooper Basin. Of Kapel (1972). Oil and gas reserves. Peat swamp and flood-plain facies. Thickness from >42 to ~285m. Early Permian. Tectonism discussed. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation and Tirrawarra Sandstone. Is overlain by Hutton Sandstone, Epsilon Formation and conformably by Murteree Shale.|Grey, buff or brown, fine- to medium-grained, locally coarse-grained and pebbly, sandstone; grey-brown to dark grey siltstone and mudstone, thinly bedded or laminated; inertinite-rich coal laminations, thin seams and beds, locally 16m thick in the N.|
14936|Patchawarra Formation|69454|5|Briefly described|p38:4, 6, 13|Cisuralian|Cisuralian|Cooper Basin. Potential seal for underlying Tirrawarra Sandstone reservoirs.||Gidgealpa Group.||Lateral equivalent of Purni Formation.||12-JUL-16
14936|Patchawarra Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
14936|Patchawarra Formation|69673|6|Mentioned|p151, p153 fig 125|||||Gidgealpa Group||Overlain by Murteree Shale, Epsilon Formation, overlies Tirrawarra Sandstone||
14936|Patchawarra Formation|69728|6|Mentioned|p285|||Cooper Basin.||Gidgealpa Group.||||
14936|Patchawarra Formation|69797|5|Briefly described|p16, p17 Fig.2|Early Permian|Early Permian|Coal and carbonaceous shale of Patchawarra Formation represent principal source rocks of Cooper Basin, both in source richness and quality, and overall thickness. Age: Asselian - Artinskian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group|||Shales and coals.|17-JAN-17
14936|Patchawarra Formation|69946|5|Briefly described|p9, p36, p45, p54|Artinskian|Asselian|Cooper Basin. Peat swamp and floodplain facies.||Unit in Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
14936|Patchawarra Formation|69982|5|Briefly described|p15, p44, p65, p72, p87, p91, p94, p102|||See also p106, p108. Cooper Basin. Source rocks for hydrocarbons which have migrated to Warburton Basin units. Brief thin section descriptions.||||||
14936|Patchawarra Formation|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale.||
14936|Patchawarra Formation|70823|4|Described|iv, p1-p3, p6, p15, 53-58|Kungurian|Sakmarian|Cooper Basin. Hosts deep, dry coal seam gas. Seismic reflection and outcrop characteristics are briefly discussed. Up to 680m thick but with an average thickness of 130m. Deposited in fluviolacustrine, floodplain and minor deltaic environments. Hosts the most significant gas-condensate reservoirs in the Cooper Basin; these are discussed briefly. See also p25-p27, p38, p40-p41, p51, p61, p66, p70, p72, p78-p80, p82-p83. Age based on palynology APP2.1 - APP3.2.||Gidgealpa Group||Overlies and interfingers with the Tirrawarra Sandstone. Conformably overlain by, or intertongues with the Murteree Shale. Unconformably overlain by the Toolachee Formation.|Interbedded sandstone, siltstone, shale and coal.|22-AUG-18
14936|Patchawarra Formation|70824|4|Described|p1-p3, p5, p7-p9, p14, p18-p20, |Kungurian|Sakmarian|Cooper Basin. Together with the Toolachee Formation these are the richest, thickest and most extensive source rocks. Hosts deep dry coal seam gas. Average thickness up to 130m but in the Nappamerri Trough reaches thicknesses in excess of 680m. Deposited under fluviolacustrine, floodplain and deltaic conditions. Source rock geochemistry and outcrop and areal extent discussed. See also p27 fig 3.7, p28-p33, p48-p59, p66, p84, p108-p110, p113, p122.||||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.|Interbedded sandstone, siltstone, shale and coal. Sandstones are dominantly quartzose, fine to medium-grained and locally coarse-grained.|
14936|Patchawarra Formation|70946|5|Briefly described|p1087, p1089-1091|Permian|Early Permian|Cooper Basin. Hosts shallow and deep dry coal seam gas accumulations. Contains a number of non-marine units. Deposited in peat swamp, fluvio-deltaic and lacustrine environments.||Gidgealpa Group.||Is overlain by Murteree Shale.||08-OCT-18
14936|Patchawarra Formation|71265|5|Briefly described|p589|Kungurian|Sakmarian|Cooper Basin.||Gidgealpa Group.||Overlies Tirrawarra Sandstone. Is overlain by Murteree Shale; locally Epsilon Formation (equivalent).||
14936|Patchawarra Formation|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36|Kungurian|Sakmarian|Cooper Basin. Deposited in a peat swamp, fluvio-deltaic, lacustrine or floodplain environment. Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p45, Ch5 p54, Ch7 p13, Ch10 tbl 10.1, Ch10 p7-p9, Ch10 p14-p15, Ch10 p17-p20, Ch13 p9.||Gidgealpa Group||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.||
14936|Patchawarra Formation|71701|5|Briefly described|p155, p170|Kungurian|Sakmarian|Cooper Basin.||Gidgealpa Group||Overlies the Tirrawarra Sandstone. Overlain by the Murteree Shale.||
14936|Patchawarra Formation|72297|5|Briefly described|p697, p739, p742|Permian|Permian|Cooper Basin. Contains coal, but at too great a depth for economic extraction. One of the main petroleum source rocks within the Basin; also a reservoir. Also contains the largest reservoired gasfield in QLD, at Stokes.||||||
14936|Patchawarra Formation|72497|6|Mentioned|p13.|||Cooper Basin. Oil and gas in Tirrawarra Sandstone and Merrimelia Formation believed to be sourced from this formation (Taylor et al., 1988).||||Overlies Tirrawarra Sandstone.|Includes coals.|
14936|Patchawarra Formation|73167|5|Briefly described|p662, p664, p677|middle Permian|middle Permian|Cooper Basin. Deposited in cycles of fluvio-deltaic, lacustrine and swamp conditions. Contains gas, hydrocarbon source. Onlap in the middle part is attributed to the NW-SE compressional mid-Permian event. NW-SE striking strike-slip faults terminate in the middle Patchawarra Formation. Referred to as middle Patchawarra Formation p677, and as Middle Patchawarra Formation on p662.|||Moorari Beds, VC Coal [?]||Sandstones, shales and thick coals.|
14936|Patchawarra Formation|73244|5|Briefly described|p83-95|Permian|Permian|Cooper Basin. Gas-rich source rock; most prolific source and reservoir unit in the basin; major exploration target. NMR analysis was conducted to create pseudo-capillary pressure curves. Recurring fluvio-deltaic, lacustrine and swamp conditions.|||||Cycles of sandstone, siltstone and coals that range in thickness from less than 1 m to tens of metres.|
14936|Patchawarra Formation|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Lacustrine, fluviodeltaic, and peat swamp depositional environments. Hydrocarbon source rock that contains[?] gas and oil.||Gidgealpa Group||Underlain by Tirrawarra Sandstone. Overlain by Murteree Shale.||
14936|Patchawarra Formation|73343|5|Briefly described|p336-338, p341-345|Permian|Permian|Cooper Basin. Gas-rich and low permeability source rock. [The name Middle Patchawarra Formation appears to be used in reference to a seismic reflector/surface/horizon]. [Article includes a detailed investigation of subsurface fracture networks].|||VC Coal and Moorari Beds.|Underlain by Tirrawarra Formation. Overlain by Epsilon Formation and Murteree Shale.|May include sand, shale, and coal.|
14936|Patchawarra Formation|73479|4|Described|p156-p157, p159-161, p163-166, p178|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine/swamp depositional environment. Gas-rich. Intra-formational on-lapping along paleo-structural highs during deposition. Deposition ended with east to west transgression.|ca 285-260 Ma||VC Coal, Moorari Beds|Overlies Tirrawarra Formation, underlies Epsilon Formation, Murteree Shale|Repeated cycles of thick sandstone, shale, and coal. Finer-grained and more shale-dominated in upper part.|
14936|Patchawarra Formation|73495|5|Briefly described|p497, p499-500, p502-506|Kungurian|Artinskian|Of Kapel (1972). Cooper Basin. New CA-TIMS zircon ages from tuffs ranging between 284.87 +/- 0.07/0.16/0.34 Ma and 277.36 +/- 0.04/0.14/0.33 Ma. Basal contact may represent an unconformity. Contains conventional oil and gas accumulations and unconventional gas in tight sandstones and deep coals. Also underlain by basement. Varies substantially in thickness across the basin up to at least 680 m. Reflects fluvial channels, lakes, floodplains, gentle uplands, and raised mire settings. Several informal subdivision schemes have been proposed. Includes several tuffs between 1 and 8 cm thick.|ca 284.87-277.36 Ma U-Pb CA-TIMS|Gidgealpa Group||Underlain by the Tirrawarra Sandstone and unconformably by Merrimelia Formation. Overlain by Murteree Shale.|Locally coarse-grained and pebbly sandstone, fine- to medium-grained sandstone, siltstone, mudstone and coal beds.|
14961|Peace Sandstone|40954|6|Mentioned|p132|||||||||
14961|Peace Sandstone|41034|6|Mentioned|p374|||||||||
14970|Peak Range Volcanics|32493|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14970|Peak Range Volcanics|33705|6|Mentioned|p48|||||||||
14970|Peak Range Volcanics|34389|4|Described|Table 2|||Tertiary||||||
14970|Peak Range Volcanics|34408|6|Mentioned|p185|||On Table||||||
14970|Peak Range Volcanics|37607|6|Mentioned|Fig.8|||||||||
14970|Peak Range Volcanics|37859|6|Mentioned|p69|||||||||
14970|Peak Range Volcanics|39212|4|Described|p31|||Olig.- Mioc.||||||
14970|Peak Range Volcanics|39445|5|Briefly described|Table 14|||||||||
14970|Peak Range Volcanics|41246|6|Mentioned|Map legend|Tertiary||||||||
14970|Peak Range Volcanics|43204|5|Briefly described|Map Legend|Oligocene|Paleocene|||||||23-DEC-11
14970|Peak Range Volcanics|43213|4|Described|p74, p151, p163-164|Oligocene|Oligocene|Tertiary. Constitutes the Fletchers Awl intrusion. A series of prominent plugs and volcanic centres with a NW trend, the Peak Range lineament: a direct continuation of the Saint Anns Megashear.|31.5-27 Ma (Wellman and McDougall, 1974).|||Intrudes Greybank Volcanics.|Rhyolite dykes and circular intrusions, commonly with glassy selvedges; restricted flows and minor tuff.|
14970|Peak Range Volcanics|43994|14|Not recorded|Map Legend|||||||||
14970|Peak Range Volcanics|43998|4|Described|p15,16,map||Tertiary|26+/-2 Ma.||||||
14970|Peak Range Volcanics|44331|14|Not recorded|Map Legend||Tertiary|||||||
14970|Peak Range Volcanics|44337|5|Briefly described|Map Legend||Tertiary|Lithology.||||||
14970|Peak Range Volcanics|45071|3|Fully described|Table 16|||See also p88.||||||30-SEP-22
14970|Peak Range Volcanics|45087|5|Briefly described|p88|||Chemical analyses||||||
14970|Peak Range Volcanics|48843|2|Defined|p44,49,51,55-59,map||Tertiary|?Tert., "a suite of peralkaline trachytic and rhyolitic domes, plugs, dykes, other intrusions and minor flows".||||||
14970|Peak Range Volcanics|48845|2|Defined|p44,49,51,55-59,map||Tertiary|"A suite of peralkaline trachytic and rhyolitic domes, plugs, dykes, other intrusions and minor flows."||||||
14970|Peak Range Volcanics|61155|5|Briefly described|p20|Late Oligocene|Early Oligocene|In the Fitzroy region.||||||
14970|Peak Range Volcanics|65455|6|Mentioned|p7|Phanerozoic|Phanerozoic|In the Bowen Basin. Noteworthy in terms of their U content.||||||09-MAY-12
14970|Peak Range Volcanics|66084|5|Briefly described|Map legend|Tertiary|Tertiary|Alkaline trachyte and rhyolite; plugs, domes and flows.||||||
14970|Peak Range Volcanics|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran, Gin Gin and Mount Runsome Basalts; Main Range, Minerva Hills and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
14970|Peak Range Volcanics|73037|5|Briefly described|Map legend|Oligocene|Oligocene||||||Alkaline trachyte and rhyolite; plugs, domes and flows.|
14970|Peak Range Volcanics|73450|4|Described|p1-2, p4-5, p79-81|Rupelian|Rupelian|Form two distinct clusters of rhyolite and trachyte peaks and domes between Clermont and Dysart. Individual domes are known to be enriched in rare-earth elements and other critical metals. Overall distribution suggests presence of two overlapping volcanoes (Cohen, 2007). The northern cluster of felsic rocks is dominantly peraluminous rhyolite whereas the southern cluster comprises mainly metaluminous trachyte and peralkaline rhyolite and trachyte (Mollan, 1965). Ages range from 31.6 +/- 1.2 Ma to 27.4 +/- 11 Ma (K-Ar and Ar-Ar).|ca 30 Ma||||Extremely porphyitic to aphyric rhyolite with flow banding and lithophysae, phonolite, tuffs, augite trachyte, hornblende trachyte and rhyolite, sodic amphibole rhyolite, and aegirine rhyolite.|
14984|Peawaddy Formation|13516|5|Briefly described|p145 fig 3, p146 fig 4, p152 fig 6, p156|Late Permian|Late Permian|From Denison Trough, Bowen Basin, also Galilee Basin. Age APP5004 - APP5005||||||
14984|Peawaddy Formation|22601|6|Mentioned|414, 418|||Geol province Bowen Basin. Overlying unit Black Alley Shale||||||
14984|Peawaddy Formation|22872|6|Mentioned|p535, Fig.1 p536|||Informally divided into Upper and Lower Peawaddy Formation.||||||
14984|Peawaddy Formation|22973|5|Briefly described|p11 Fig.2(f)|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|22975|5|Briefly described|p34 Fig.6|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|22976|5|Briefly described|p42 Fig.4|Permian|Permian|||||||
14984|Peawaddy Formation|22978|6|Mentioned|p148 Fig.1|||||||||
14984|Peawaddy Formation|22980|5|Briefly described|p249 Fig.2|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
14984|Peawaddy Formation|23444|5|Briefly described|p190 Fig. 6|Permian|Permian|||||||
14984|Peawaddy Formation|24071|5|Briefly described|p317 Table 1|Late Permian|Early Permian|Geological Province: Galilee Basin.||||||
14984|Peawaddy Formation|24077|5|Briefly described|p410 Tb. 2||Late Permian|Of the Blenheim Subgroup.  Together with the Mantuan Productus Bed, consists of mudstone, sandstone and coal; sandstone both lithic and orthoquartzitic, coquinite, thin limestone and mudstone at top.  Max. thickness; 210m. Geological Prov: Bowen Basin.||||||
14984|Peawaddy Formation|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Age: ~259Ma.  Geological Province: Bowen Basin.||||||
14984|Peawaddy Formation|29391|6|Mentioned|Table 3|||See P18.||||||
14984|Peawaddy Formation|29393|6|Mentioned|Table 2|||Permian.||||||
14984|Peawaddy Formation|29409|6|Mentioned|Table 1|||Correlation.||||||
14984|Peawaddy Formation|29410|6|Mentioned|p274|||Geological map. Permian.||||||
14984|Peawaddy Formation|29411|5|Briefly described|p201|||||||||
14984|Peawaddy Formation|29436|6|Mentioned|p317|||||||||
14984|Peawaddy Formation|29437|6|Mentioned|p156|||||||||
14984|Peawaddy Formation|29721|6|Mentioned|Table 65|||||||||
14984|Peawaddy Formation|30153|6|Mentioned|p151|||||||||
14984|Peawaddy Formation|30155|6|Mentioned|p464|||||||||
14984|Peawaddy Formation|30340|6|Mentioned|p2532|||||||||
14984|Peawaddy Formation|30341|5|Briefly described|p136|||Upper Permian age||||||
14984|Peawaddy Formation|30449|6|Mentioned|p4|||Correlation with Ingelara Formation. See also P8,20||||||
14984|Peawaddy Formation|30450|6|Mentioned|Table 1|||Permian age||||||
14984|Peawaddy Formation|30508|6|Mentioned|p91|||Palynology projects||||||
14984|Peawaddy Formation|30545|6|Mentioned|Fig.2|||Part of Blenbein Subgroup||||||
14984|Peawaddy Formation|30546|6|Mentioned|p107|||Correlation. Upper Permian age||||||
14984|Peawaddy Formation|30691|4|Described|p14|||See also P20,Table 3. Upper Permian age||||||
14984|Peawaddy Formation|30696|4|Described|Table 3|||Lower to Upper Permian||||||
14984|Peawaddy Formation|30826|6|Mentioned|p634|||||||||
14984|Peawaddy Formation|30854|6|Mentioned|p8|||||||||
14984|Peawaddy Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
14984|Peawaddy Formation|30915|6|Mentioned|p99|||||||||
14984|Peawaddy Formation|30916|6|Mentioned|p98|||||||||
14984|Peawaddy Formation|31115|6|Mentioned|p32|||Permian||||||
14984|Peawaddy Formation|31120|4|Described|p152|||||||||
14984|Peawaddy Formation|31122|6|Mentioned|p352|||||||||
14984|Peawaddy Formation|31260|6|Mentioned|p16|||Refers facies analysis||||||
14984|Peawaddy Formation|31303|5|Briefly described|p292|||See also Table 1||||||
14984|Peawaddy Formation|31304|5|Briefly described|p628|||Lithology in drill hole.||||||
14984|Peawaddy Formation|31305|4|Described|p568|||Mention Table 1||||||
14984|Peawaddy Formation|31531|5|Briefly described|p11|||See also Table 1. U.Permian||||||
14984|Peawaddy Formation|31656|6|Mentioned|Table 1|||Part equiv. to Maria Fm.||||||
14984|Peawaddy Formation|32096|6|Mentioned|p574|||||||||
14984|Peawaddy Formation|32139|6|Mentioned|p583|||||||||
14984|Peawaddy Formation|32193|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
14984|Peawaddy Formation|32493|6|Mentioned|Map legend|Middle Permian|Early Permian|Lower - Middle Permian||||||
14984|Peawaddy Formation|32577|5|Briefly described|p23|||U.Perm. See also P24,27,33.||||||
14984|Peawaddy Formation|32578|6|Mentioned|p348|||Refers Swindon (1968)||||||
14984|Peawaddy Formation|32689|6|Mentioned|Fig.2|||Refers Power (1967)||||||
14984|Peawaddy Formation|32840|6|Mentioned|p1|||Stratigraphy & biostratigraphy. See P30||||||
14984|Peawaddy Formation|32944|6|Mentioned|p710|||Permian||||||
14984|Peawaddy Formation|32945|6|Mentioned|p81|||See also PP82,90 & Fig.3.||||||
14984|Peawaddy Formation|33059|4|Described|Table 1|||L.Perm.||||||
14984|Peawaddy Formation|33078|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|33079|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|33086|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|33092|5|Briefly described|p7|||Strat. table||||||
14984|Peawaddy Formation|33096|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|33366|6|Mentioned|Fig.3|||Perm.||||||
14984|Peawaddy Formation|33369|6|Mentioned|p214|||Strat. succession in GSQ Jericho 1.||||||
14984|Peawaddy Formation|33530|5|Briefly described|Table 1|||Upper Perm.||||||
14984|Peawaddy Formation|33639|6|Mentioned|Fig.1|||||||||
14984|Peawaddy Formation|33640|5|Briefly described|Table 4|||||||||
14984|Peawaddy Formation|33646|5|Briefly described|Table 3|||Palynological stage.||||||
14984|Peawaddy Formation|33648|6|Mentioned|p17|||Palynological divisions.||||||
14984|Peawaddy Formation|33675|4|Described|p411|||Lithology.||||||
14984|Peawaddy Formation|33701|6|Mentioned|Fig.1|||Kazanian.||||||
14984|Peawaddy Formation|33711|6|Mentioned|Table 3|||||||||
14984|Peawaddy Formation|33745|6|Mentioned|Fig.6|||See also Fig.7.||||||
14984|Peawaddy Formation|33993|6|Mentioned|p310|||Permian. Brachiopod shells.||||||
14984|Peawaddy Formation|34132|6|Mentioned|p2|||Upper Permian||||||
14984|Peawaddy Formation|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
14984|Peawaddy Formation|34174|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|34392|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
14984|Peawaddy Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
14984|Peawaddy Formation|35079|6|Mentioned|Fig.3|||||||||
14984|Peawaddy Formation|35148|4|Described|p414|||See also Table 1.||||||
14984|Peawaddy Formation|35150|6|Mentioned|p420|||||||||
14984|Peawaddy Formation|35238|6|Mentioned|Fig.4|||||||||
14984|Peawaddy Formation|35284|6|Mentioned|Fig.1|||||||||
14984|Peawaddy Formation|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
14984|Peawaddy Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
14984|Peawaddy Formation|35845|6|Mentioned|Fig.25|||||||||
14984|Peawaddy Formation|35873|6|Mentioned|Fig.25|||||||||
14984|Peawaddy Formation|35901|6|Mentioned|p2|||||||||
14984|Peawaddy Formation|36103|4|Described|Table 1|||||||||
14984|Peawaddy Formation|36104|6|Mentioned|p122|||||||||
14984|Peawaddy Formation|36233|5|Briefly described|p157|||See also Table 1.||||||
14984|Peawaddy Formation|36241|4|Described|p123|||||||||
14984|Peawaddy Formation|36243|6|Mentioned|Table 3A|||||||||
14984|Peawaddy Formation|36739|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|36921|6|Mentioned|p175|||||||||
14984|Peawaddy Formation|37070|6|Mentioned|p69|||||||||
14984|Peawaddy Formation|37072|6|Mentioned|p91|||||||||
14984|Peawaddy Formation|37450|6|Mentioned|p374|||||||||
14984|Peawaddy Formation|37610|6|Mentioned|Fig.3|||||||||
14984|Peawaddy Formation|37705|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|37724|6|Mentioned|Table 1|||||||||
14984|Peawaddy Formation|37726|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|37918|6|Mentioned|p474|||||||||
14984|Peawaddy Formation|38092|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|38198|6|Mentioned|p414|||||||||
14984|Peawaddy Formation|38204|6|Mentioned|p80|||||||||
14984|Peawaddy Formation|38312|4|Described|p462|||||||||
14984|Peawaddy Formation|38374|6|Mentioned|p602|||||||||
14984|Peawaddy Formation|38955|4|Described|p314|||||||||
14984|Peawaddy Formation|39212|4|Described|p34|||Excursion site described. P24 gas reservoir. See also P11,13,35||||||
14984|Peawaddy Formation|39219|6|Mentioned|p46|||Microflora||||||
14984|Peawaddy Formation|39252|6|Mentioned|Fig.13|||||||||
14984|Peawaddy Formation|39261|6|Mentioned|Fig.6|||||||||
14984|Peawaddy Formation|39263|6|Mentioned|Fig.1|||||||||
14984|Peawaddy Formation|39264|6|Mentioned|Fig. 4|||||||||
14984|Peawaddy Formation|39267|6|Mentioned|p238|||See also P239||||||
14984|Peawaddy Formation|39268|6|Mentioned|p270|||||||||
14984|Peawaddy Formation|39272|5|Briefly described|p295|||Correlation||||||
14984|Peawaddy Formation|39273|5|Briefly described|p309|||||||||
14984|Peawaddy Formation|39275|6|Mentioned|p332|||||||||
14984|Peawaddy Formation|39412|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|39423|6|Mentioned|p47|||||||||
14984|Peawaddy Formation|39445|5|Briefly described|Table 8|||||||||
14984|Peawaddy Formation|39494|6|Mentioned|Fig.5|||||||||
14984|Peawaddy Formation|39815|6|Mentioned|Fig.10|||||||||
14984|Peawaddy Formation|39943|6|Mentioned|Table 5A|||||||||
14984|Peawaddy Formation|40030|6|Mentioned|p135|||||||||
14984|Peawaddy Formation|40093|6|Mentioned|p31|||See also P40||||||
14984|Peawaddy Formation|40123|6|Mentioned|Fig.3|||||||||
14984|Peawaddy Formation|40250|6|Mentioned|Table 6|||||||||
14984|Peawaddy Formation|40256|6|Mentioned|Fig.4|||||||||
14984|Peawaddy Formation|40321|6|Mentioned|p21|||See also Fig.4||||||
14984|Peawaddy Formation|40539|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|40544|6|Mentioned|Fig.6|||||||||
14984|Peawaddy Formation|41173|6|Mentioned|Table 2|||||||||
14984|Peawaddy Formation|41246|6|Mentioned|Map legend|Permian||||||||
14984|Peawaddy Formation|41247|6|Mentioned|Fig.7|||||||||
14984|Peawaddy Formation|41330|6|Mentioned|Table 1|||||||||
14984|Peawaddy Formation|41475|6|Mentioned|p70|||||||||
14984|Peawaddy Formation|41514|6|Mentioned|p83|||||||||
14984|Peawaddy Formation|41605|6|Mentioned|Fig.2|||||||||
14984|Peawaddy Formation|41666|6|Mentioned|P|||||||||
14984|Peawaddy Formation|41809|6|Mentioned|p71|||||||||
14984|Peawaddy Formation|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
14984|Peawaddy Formation|42091|6|Mentioned|Text fig.2 P284|||||||||
14984|Peawaddy Formation|42249|6|Mentioned|p23|||||||||
14984|Peawaddy Formation|42250|6|Mentioned|Fig.4 P31|||||||||
14984|Peawaddy Formation|42253|5|Briefly described|Fig.2 P217|||||||||
14984|Peawaddy Formation|42254|6|Mentioned|p221|||||||||
14984|Peawaddy Formation|42437|6|Mentioned|Fig.3 P822|||||||||
14984|Peawaddy Formation|42578|5|Briefly described|Table 1 P124-125|||||||||
14984|Peawaddy Formation|42641|5|Briefly described|p108|||||||||
14984|Peawaddy Formation|42662|6|Mentioned|p84 Fig.4|||||||||
14984|Peawaddy Formation|42856|5|Briefly described|Fig.2 P632|||||||||
14984|Peawaddy Formation|42911|5|Briefly described|p10|||||||||
14984|Peawaddy Formation|42994|6|Mentioned|p273|||||||||
14984|Peawaddy Formation|43000|5|Briefly described|p113|||see also Fig.5,p112||||||
14984|Peawaddy Formation|43017|5|Briefly described|Fig.3,p375|||||||||
14984|Peawaddy Formation|43050|5|Briefly described|p4|||see also Fig.1,p5.||||||
14984|Peawaddy Formation|43105|6|Mentioned|p13|||||||||
14984|Peawaddy Formation|43185|5|Briefly described|6-10||Late Permian|||||||
14984|Peawaddy Formation|43471|14|Not recorded|p229|||Megadesmus, Astartila||||||
14984|Peawaddy Formation|43474|14|Not recorded|p7,9,39,52,66,86||Late Permian|||||||
14984|Peawaddy Formation|43475|14|Not recorded|p553||Permian|||||||
14984|Peawaddy Formation|43580|6|Mentioned|p360||Permian|||||||
14984|Peawaddy Formation|43714|6|Mentioned|Fig.3,p5||Late Permian|||||||
14984|Peawaddy Formation|43737|6|Mentioned|p5|||||||||
14984|Peawaddy Formation|43812|6|Mentioned|Fig.3,p145|||||||||
14984|Peawaddy Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
14984|Peawaddy Formation|43886|14|Not recorded|p184||Permian|||||||
14984|Peawaddy Formation|43977|2|Defined|p576-579,580|||||||||
14984|Peawaddy Formation|43982|14|Not recorded|Map Legend|||||||||
14984|Peawaddy Formation|43989|14|Not recorded|Map Legend||Late Permian|||||||
14984|Peawaddy Formation|43990|14|Not recorded|Map Legend|||Part of the Blenheim Sub-Group.||||||
14984|Peawaddy Formation|43994|14|Not recorded|Map Legend|||||||||
14984|Peawaddy Formation|44022|14|Not recorded|Map Legend||Late Permian|||||||
14984|Peawaddy Formation|44023|4|Described|Tb.2,p7||Late Permian|||||||
14984|Peawaddy Formation|44091|14|Not recorded|p45|||Part of Middle Bowen Group in Springsure area.||||||
14984|Peawaddy Formation|44169|14|Not recorded|Tb.1,p6,7,12,13,map|||||||||
14984|Peawaddy Formation|44170|4|Described|p6,11,29,30,33,Tb.1||Late Permian|Includes Mantuan Productus Bed. Tb.3||||||
14984|Peawaddy Formation|44172|2|Defined|p1323,1327,1330-4,||Kazanian|Gas. p1337,1341-3,Fig.2,Tb.1||||||
14984|Peawaddy Formation|44173|14|Not recorded|p110,112||Late Permian|||||||
14984|Peawaddy Formation|44218|14|Not recorded|p19||Sakmarian|||||||
14984|Peawaddy Formation|44219|14|Not recorded|p31||Kazanian|||||||
14984|Peawaddy Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
14984|Peawaddy Formation|44381|14|Not recorded|p5|||||||||
14984|Peawaddy Formation|44419|14|Not recorded|p272,273,275||Permian|||||||
14984|Peawaddy Formation|44421|14|Not recorded|p6,8,9||Permian|||||||
14984|Peawaddy Formation|44422|14|Not recorded|p150,152,153|||= Mantuan Productus Bed + "Dry Creek Shale".||||||
14984|Peawaddy Formation|44424|14|Not recorded|p293-301|||Part of Blenheim Subgroup.||||||
14984|Peawaddy Formation|44426|14|Not recorded|p11|||Springsure area.||||||
14984|Peawaddy Formation|44427|1|Redefined|p165|||Upper part equivalent to Mantuan Productus Bed, lower part equivalent to redefined Oxtrack Formation.||||||
14984|Peawaddy Formation|44512|14|Not recorded|p16|||Fauna.||||||
14984|Peawaddy Formation|44618|14|Not recorded|p511,515-518,520||Permian|||||||
14984|Peawaddy Formation|44787|14|Not recorded|p124||Late Permian|||||||
14984|Peawaddy Formation|45006|14|Not recorded|p6,7|||||||||
14984|Peawaddy Formation|45031|14|Not recorded|p9,11,89,Fig.3,||Permian|||||||
14984|Peawaddy Formation|45071|3|Fully described|Table 10|||See also p55.||||||23-OCT-19
14984|Peawaddy Formation|45073|6|Mentioned|p58|||Geological history||||||
14984|Peawaddy Formation|46849|6|Mentioned|Fig. 7|||||||||
14984|Peawaddy Formation|46989|5|Briefly described|Table 1|||||||||
14984|Peawaddy Formation|48898|6|Mentioned|Fig.4|||See also PP27,38. U.Permian||||||
14984|Peawaddy Formation|48900|3|Fully described|p37|||||||||
14984|Peawaddy Formation|48919|5|Briefly described|p18|||Upper Permian.||||||
14984|Peawaddy Formation|48920|3|Fully described|p26|||Upper Permian age||||||
14984|Peawaddy Formation|48995|6|Mentioned|Fig.3|||||||||
14984|Peawaddy Formation|49644|5|Briefly described|Table|||||||||
14984|Peawaddy Formation|60115|5|Briefly described|p21 Fig. 1|Late Permian|Late Permian|Geological Province: Bowen Basin/Comet Ridge.||||||04-FEB-08
14984|Peawaddy Formation|60286|4|Described|p277|Late Permian|Late Permian|Overlies Catherine Sandstone and German Creek Formation. Overlain by Black Alley Shale. Prograding birdsfoot delta deposit. Geological Province: Bowen Basin.||||||
14984|Peawaddy Formation|60330|5|Briefly described|p259|Late Permian|Late Permian|Includes silty dark grey shales. Slightly fossiliferous. Geological Province: Denison Trough.||||||
14984|Peawaddy Formation|61609|6|Mentioned|p240|Permian|Permian|Underlain by Catherine Sandstone. Geological Province: Denison Trough.||||||07-FEB-11
14984|Peawaddy Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Age: c. 266Ma. Geological Province: Bowen Basin.||||||17-MAR-09
14984|Peawaddy Formation|61778|5|Briefly described|p239||Late Permian|Geological Province: Bowen Basin.||||||07-FEB-11
14984|Peawaddy Formation|62357|5|Briefly described|p524 Fig. 7|Late Permian|Late Permian|Geological Province: Bowen Basin.||||||
14984|Peawaddy Formation|63172|6|Mentioned|p307|||Queensland stratigraphic unit.||||||07-FEB-11
14984|Peawaddy Formation|63713|5|Briefly described|p1507-1508, p1523, p1526, p1528-1533|Capitanian|Wordian|Eastern margin, Galilee Basin; Denison Trough, Bowen Basin. Graphic log. Well-log correlation.||||Overlies Colinlea Sandstone. Is overlain by Black Alley Shale. Correlated with Tinowon Formation.|Heterolithic mudrocks and sandstones, locally showing coarsening-upward trends.|
14984|Peawaddy Formation|63832|5|Briefly described|p131 fig 2, p137|Guadalupian|Guadalupian|Of Galilee Basin and west Bowen Basin. Contains distal glaciomarine facies (outsized basement clasts in mudrock, glendonites) recording the final (P4) Paleozoic glaciation.|||||Base of this unit is dominated by first cycle volcanics.|13-DEC-17
14984|Peawaddy Formation|64288|5|Briefly described|p532 Fig.1 |Campanian|Wordian|||||Overlies Colinlea Sandstone. Is overlain by Black Alley Shale.||
14984|Peawaddy Formation|64631|5|Briefly described|p44 Fig.2, p48 Fig.4, p49.|Capitanian|Capitanian|Galilee and Bowen Basins. Contains distal glaciomarine facies, eg glendonites, and outsized basement clasts in mudrocks. Biostratigraphic age control for base and top.||||Overlies Colinlea Sandstone. Is overlain by Black Alley Shale.||
14984|Peawaddy Formation|64856|5|Briefly described|p65|Late Permian||Underlies the Black Alley Shale in the Denison Trough.|| ||||31-JAN-13
14984|Peawaddy Formation|64857|5|Briefly described|p121, p113 Fig.3|Late Permian|Late Permian|Bowen Basin. Overlies Catherine Sandstone.||||||
14984|Peawaddy Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Denison Trough, Bowen Basin. Underlies Black Alley Shale and overlies Catherine Formation.||||||22-MAR-12
14984|Peawaddy Formation|65113|5|Briefly described|p349, Fig 4 p340|Late Permian|Late Permian.|In the Denison Trough. Allen and Fielding (2007) considered this to be time equivalent to Flat Top Formation, but this paper interprets the Flat Top Formation to be older than Peawaddy. Overlies the Catherine Formation?, underlies the Black Alley Shale.||||||15-JUL-13
14984|Peawaddy Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
14984|Peawaddy Formation|65115|5|Briefly described|p415, 416, 418, 419, Fig 2 p403|Tatarian|Tatarian|Marine mudstone. Overlies the Catherine Sandstone, underlies the Black Alley Shale, in the Denison Trough, Bowen Basin. Part of Supersequence E.||||||
14984|Peawaddy Formation|65116|5|Briefly described|Fig 2 p436|Late Permian|Late Permian|Underlies the Black Alley Shale, overlies the Catherine Formation in the Denison Trough, Bowen Basin.||||||06-MAR-12
14984|Peawaddy Formation|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Black Alley Shale, ? overlies the Catherine Sandstone in the Denison Trough, Bowen Basin.||||||
14984|Peawaddy Formation|65388|6|Mentioned|p170, 172|||south west Bowen Basin. Correlated with Barfield Formation, lower Flat Top Formation||||||
14984|Peawaddy Formation|66188|6|Mentioned|431|||||||||
14984|Peawaddy Formation|66615|6|Mentioned|p2 Fig.1, p3-6|||Denison Trough, Bowen Basin.||||||
14984|Peawaddy Formation|67133|5|Briefly described|p5, p8-9, p18|Permian|Permian|Samples of this unit were analysed by XRD and optical microscopy for this study. The substantial concentration of finely disseminated marcasite suggests a marine origin, not previously described in the Bowen Basin. Middle Permian; considered Jurassic by Heywood (1977) due to similarity with overlying Precipice Sandstone.||Back Creek Group.||Is overlain by Precipice Sandstone.|Dominantly fine-grained sandstones.|
14984|Peawaddy Formation|67402|4|Described|p21, p23 fig CTM3, p64|Wuchiapingian|Wuchiapingian|Bowen Basin. Maximum thickness of 348m. Deposited in a fluvial-deltaic environment or a marine environment. Shales and siltstones form an effective reservoir for the underlying Catherine Sandstone. See also  p65, p66 fig BWW4, p68, p69, p71-p73, p78, p79, p135 fig GLL18, GLL19, p303.|||Includes the Mantuan Formation.|Overlain by the Bandanna Formation and Black Alley Shale. Overlies the Catherine Sandstone, Ingelara Formation and Freitag Formation.|Interbedded siltstone, shale, sandstone and minor coal.|
14984|Peawaddy Formation|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Black Alley Shale/Winnathoola CM. Underlain by Catherine Sandstone/Ingelara Formation.||
14984|Peawaddy Formation|68279|5|Briefly described|p2, p4, p5 Tb.2, p7-9, p16 Tb.4, p18-19|Lopingian|Lopingian|Galilee Basin. Significant concentration of pyrite suggests prolonged marine influence. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Overlies Colinlea Sandstone. Is overlain by Black Alley Shale.|Includes light grey, fine-grained, well-sorted sandstone; fine-grained grey-brown interbedded siltstone and dark grey massive mudstone.|
14984|Peawaddy Formation|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||Of the Back Creek Group.||Conformably overlain by the Black Alley Shale. Conformably underlain by the Colinlea Sandstone.|Mudstone, siltstone, sandstone, and coquinite.|
14984|Peawaddy Formation|68414|5|Briefly described|Map Legend|Permian|Permian|Bowen Basin.||Of the Back Creek Group.||Conformably overlain by the Black Alley Shale. Conformably underlain by the Colinlea Sandstone.|Mudstone, siltstone, sandstone and coquinite.|
14984|Peawaddy Formation|68576|5|Briefly described|Q_4: p3, p10-11, p20, p24|Lopingian|Lopingian|Bowen Basin. Shallow-marine deposits.|||Mantuan Productus bed.|Overlies Catherine Sandstone. Is overlain conformably by Black Alley Shale.|Thinly interbedded and inter-laminated micaceous grey siltstone and dark carbonaceous mudstone, with abundant plant debris, worm burrows, gypsum and jarosite on bedding planes; coarse labile sandstone with large cross-beds in upper half.|
14984|Peawaddy Formation|68679|5|Briefly described|p350, p377, p381-382, p384|Permian|Permian|Mollan et al. (1964). Known as the Mantuan Formation in the petroleum industry. Denison Trough, Bowen Basin. 345m thick. Prograding delta system deposits. Mentioned as having the same fossil species as, and thus establishing the age of, the Warminster Formation (Yarrol Province). Produces gas and minor condensate.|||Mantuan Productus bed.|Overlies Ingelara Formation (in the S) and Catherine Sandstone (in the N). Is overlain by Black Alley Shale. Laterally equivalent to Fair Hill Formation.|Mudstone, siltstone, sublabile sandstone, coquinitic limestone.|
14984|Peawaddy Formation|68731|6|Mentioned|p201 Fig 3.110|Lopingian|Lopingian|Deposited under marine/deltaic/lacustrine conditions (Swarbrick 1974; Gray 1976; Allen and Fielding 2007).|||||Comprises mainly sandstone, with lesser amounts of siltstone, mudstone and coal.|17-JUL-14
14984|Peawaddy Formation|70815|6|Mentioned|p6|||||||||
14984|Peawaddy Formation|70857|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group||Overlies Colinlea Sandstone, overlain by Black Alley Shale|Mudstone, siltstone, sandstone and coquinite.|
14984|Peawaddy Formation|71265|5|Briefly described|p589-592, p596, p598, p602, p606-607|Changhsingian|Changhsingian|Bowen and eastern Galilee Basins. Contains marine sediments. 21m thick in GSQ Tambo 1-1A (sedimentary log). Facies discussed; interpreted as tidal flats deposits.||||Overlies Catherine Sandstone. Is overlain by Black Alley Shale. Interfingers with and equivalent to Colinlea Sandstone; the top coquinite is lateral equivalent to Mantuan Productus beds.|Interbedded fine-grained sandstone and mudstone drapes. Wavy and flaser bedding; local horizontal burrows. Has a coquinite at the top.|
14984|Peawaddy Formation|71276|5|Briefly described|p285-286, p288, p292-293, p295-298|Lopingian|Lopingian|Mollan et al. (1964). Galilee Basin. Used to describe the upper part of the Colinlea Sandstone (i.e. replace the Mantuan Downs Productus Bed), for sediments on the eastern Springsure Shelf. Coal seam correlation. The upper part of this unit correlates with the Fair Hill Formation.||||Overlies Colinlea Sandstone. Is overlain conformably by the Bandanna Formation or Black Alley Shale. Equivalent to the Mantuan Productus Beds. Interfingers with MacMillan Formation.||
14984|Peawaddy Formation|71701|5|Briefly described|p155, p159, p168-p169|Changhsingian|Wuchiapingian|Springsure Shelf, Galilee Basin and Denison Trough, Bowen Basin.||||Overlies the Catherine Sandstone. Overlain by the Black Alley Shale.||
14984|Peawaddy Formation|71710|6|Mentioned|p370 Fig 3, p381|Late Permian|Late Permian|Geological province: southern Galilee Basin.||||Overlain by Black Alley Shale. Underlain by Colinlea Sandstone. Deposited during marine transgression, separating Colilea Sandstone and Bandanna Formation.||
14984|Peawaddy Formation|72088|4|Described|p8, p20-p21, p38-p40, p91|Wuchiapingian|Wuchiapingian|Southern Galilee Basin and Bowen Basin. Deposited under marine to deltaic or lacustrine conditions.||||Overlies the Colinlea Sandstone. Overlain by the Black Alley Shale.|Mainly sandstone with lesser siltstone, mudstone and coal.|
14984|Peawaddy Formation|73304|6|Mentioned|p77-78|||Bowen Basin.||||||
14984|Peawaddy Formation|73305|5|Briefly described|p548, p551-552, p556 Fig.8|Late Permian|Late Permian|Bowen Basin. Denison Trough. Time equivalent to the Fair Hill Formation and Tinowon Formation. Includes marine facies.|||Mantuan Productus Beds|Equivalent to the Fair Hill Formation and Tinowon Formation.||
14984|Peawaddy Formation|73472|6|Mentioned|p115-116|Wuchiapingian|Wuchiapingian|Galilee Basin.||||Underlain by Colinlea Sandstone. Overlain by Black Alley Shale. Equivalent to Betts Creek beds.||
14984|Peawaddy Formation|73625|5|Briefly described|p1-3, p5 Fig.3, p6-7, 10, 12-15, 18-21|Permian|Permian|See also p23-24, 26. Bowen Basin. Base of this unit records onset of the Hunter-Bowen Orogeny. Formed under cold, possibly glacial ice, open-marine conditions (repeated progradation of deltas). Graphic sedimentary logs.|257-254.5 Ma.|||Overlies Catherine Sandstone and (locally) Ingelara Formation. Is overlain by Black Alley Shale. Correlates with MacMillan and Fairhill Formations.|A series of coarsening-upward, terrigenous clastic intervals. Basal dark grey mudrocks and interbedded cream-coloured tuffs. Bioturbated, shell fossil-bearing and gravel-rich sandstones at the top (Mantuan Productus Bed).|
15006|Peedee Formation|42808|6|Mentioned|p159|||||||||
15006|Peedee Formation|63056|6|Mentioned|p82|||||||||
15022|Pelican Range Formation|23032|4|Described|p18||Ordovician|||||||
15022|Pelican Range Formation|23424|4|Described|Table 8.1 Fig 8.2 p331||Ordovician|Age: Unfossiliferous but probably Ordovician because of similarities to Judea Fm. Probably faulted against Wairuna, Greenvale and Perry Creek Fms. Overlying unit Clarke River Group (u). Camel Creek Subprovince.||||||
15022|Pelican Range Formation|23430|5|Briefly described|p476|||Age uncertain, inferred to be Ordovician. Broken River Province.||||||
15022|Pelican Range Formation|23431|5|Briefly described|p541|||||||||
15022|Pelican Range Formation|23494|5|Briefly described|p9, p22 Tb. 1|Silurian|Silurian|Quartz, sandstone and shale.  Downfaulted into Greenvale Formation.  Max. thickness: <5000ft.||||||
15022|Pelican Range Formation|23498|5|Briefly described|p 23 table 1||Silurian|||||||
15022|Pelican Range Formation|23509|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Broken River Province.||||||
15022|Pelican Range Formation|23619|4|Described|p34 Table 1||Ordovician|Unfossiliferous. Faulted against Wairuna, Greenvale and Perry Creek Formations. Broken River Province.||||||
15022|Pelican Range Formation|23893|5|Briefly described|p14|Ordovician|Ordovician|Geological Province: Camel Creek Subprovince.||||||
15022|Pelican Range Formation|24074|5|Briefly described|p389 Table 1|Silurian|Late Ordovician|Maximum thickness: ?1500m.||||||
15022|Pelican Range Formation|24577|4|Described|p752 Fig. 1|Ordovician|Ordovician|Overlain by the Tribute Formation. Formation is Fm in text. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
15022|Pelican Range Formation|29445|6|Mentioned|p73|||||||||
15022|Pelican Range Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Ordovician - Devonian||||||
15022|Pelican Range Formation|31832|6|Mentioned|Table 6|||||||||
15022|Pelican Range Formation|32553|4|Described|p52|||||||||
15022|Pelican Range Formation|37575|4|Described|p181|||See also Fig.3||||||
15022|Pelican Range Formation|37727|4|Described|p80|||||||||
15022|Pelican Range Formation|39027|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
15022|Pelican Range Formation|39445|5|Briefly described|Table 4|||See also P64, P74 & Fig.6. Qu-rich flysch. Correlation||||||
15022|Pelican Range Formation|39689|6|Mentioned|p52|||||||||
15022|Pelican Range Formation|40787|6|Mentioned|p324|||||||||
15022|Pelican Range Formation|40943|6|Mentioned|p50|||||||||
15022|Pelican Range Formation|41260|4|Described|p12|||||||||
15022|Pelican Range Formation|42031|6|Mentioned|Fig.6 P763|||||||||
15022|Pelican Range Formation|42690|5|Briefly described|map legend|Early Devonian|Ordovician?|||||||
15022|Pelican Range Formation|42692|5|Briefly described|map legend|Ordovician||||||||
15022|Pelican Range Formation|42752|5|Briefly described|p45|||see also Fig.2 P46||||||
15022|Pelican Range Formation|42933|3|Fully described|p22|||||||||
15022|Pelican Range Formation|43095|5|Briefly described|Plate 2|||||||||
15022|Pelican Range Formation|43113|4|Described|Table 1 p21||Ordovician|||||||
15022|Pelican Range Formation|43213|6|Mentioned|p66|Ordovician|Ordovician|Quartzose flysch sediments, preserved as thrust slices.||||||
15022|Pelican Range Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
15022|Pelican Range Formation|43259|6|Mentioned|Appendix 1,p4.|Silurian|Late Ordovician|||||||
15022|Pelican Range Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
15022|Pelican Range Formation|44044|2|Defined|p124,125,127|||||||||
15022|Pelican Range Formation|44046|14|Not recorded|p153|||||||||
15022|Pelican Range Formation|44048|14|Not recorded|Map Legend||Silurian|||||||
15022|Pelican Range Formation|44049|14|Not recorded|Map Legend||Silurian|||||||
15022|Pelican Range Formation|44059|14|Not recorded|p442(Tb)||Early Silurian|(Middle Silurian)||||||
15022|Pelican Range Formation|44515|2|Defined|p33||Silurian|Conformably overlies Wairuna Formation. Faulted against Greenvale Formation. (Silurian,possibly middle Silurian)||||||
15022|Pelican Range Formation|45009|2|Defined|p21,40-6,52,Pl.8,13,|||Tb.6||||||
15022|Pelican Range Formation|45151|6|Mentioned|p8|||||||||
15022|Pelican Range Formation|48904|6|Mentioned|Table 1|||||||||
15022|Pelican Range Formation|61727|5|Briefly described|p942 Fig.1|Ordovician|Ordovician|Geological Province: Broken River Province/Camel Creek Subprovince.||||||
15022|Pelican Range Formation|63154|5|Briefly described|p281 Fig. 3|Early Ordovician|Early Ordovician|Geological province: Broken River Province/Camel Creek Subprovince.||||||
15022|Pelican Range Formation|67848|6|Mentioned|p3 Fig.2.|||Part of the accretionary wedge in the arc-trench gap succession involved in collisional accretion.||||||
15022|Pelican Range Formation|68339|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince. Age min: Early Silurian?|||||Quartzose arenite and mudstone, local melange; jasper; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|07-JUL-15
15022|Pelican Range Formation|68340|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince. Age min: Early Silurian?|||||Quartzose arenite and mudstone, local melange; jasper; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|07-JUL-15
15022|Pelican Range Formation|68350|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince, Broken River Province. Age min: Early Devonian?|||||Quartzose arenite and mudstone, local melange; jasper (mapped separately).|07-JUL-15
15022|Pelican Range Formation|68351|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince, Broken River Province. Age min: Early Devonian?|||||Quartzose arenite and mudstone, local melange; jasper (mapped separately).|07-JUL-15
15022|Pelican Range Formation|68480|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. The 2 facies are mapped separately. Late Ordovician? to Early Silurian? in age.|||||Quartzose arenite and mudstone, local melange; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
15022|Pelican Range Formation|68481|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. The 2 facies are mapped separately. Late Ordovician? to Early Silurian? in age.|||||Quartzose arenite and mudstone, local melange; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
15022|Pelican Range Formation|68553|6|Mentioned|Map legend; schematic diagram.|Silurian|Ordovician|Broken River Province. This unit, as well as Wairuna Formation, Tribute Hills Arenite, Carriers Well Formation and Everetts Creek Volcanics, are all mapped under the symbol, OSb.||||||
15022|Pelican Range Formation|68576|5|Briefly described|Q_11: p38-39|||Camel Creek Subprovince. Forms hilly topography. Unfossiliferous: ages poorly known; may be Ordovician.|||||Quartzose sandstone.|
15022|Pelican Range Formation|69030|6|Mentioned|p6|Ordovician|Ordovician|Camel Creek Subprovince (Broken River Province).||||||
15022|Pelican Range Formation|69079|6|Mentioned|p5|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.||||||
15022|Pelican Range Formation|69592|5|Briefly described|p251 Fig.4.35, p268-269, p277-279, p297|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province. Groups several N-trending, fault-bound belts. Separates discrete tracts of Greenvale Formation. May stratigraphically overlie Greenvale Formation. Characterised by turbiditic sandstone. Melange zones common. No age constraints; provisional Ordovician age based on lithological similarities with Judea and Wairuna Formations. Appears as Pelican Hills Formation on p278.|||||Thin to very thick beds of medium-grained quartzose sandstone; generally interbedded with thin to medium beds of mudstone; several lenses to 6km long of locally pillowed, aphyric basalt associated with jasper; rare radiolarian chert and jasper.|
15022|Pelican Range Formation|70207|6|Mentioned|p20|Silurian|Ordovician|Clarke River and/or Cairns region.||||||
15022|Pelican Range Formation|73201|4|Described|p607, p610-614, p616-618, p620|Early Ordovician|Cambrian|Mossman Orogen, Broken River Province. Geochron are U-Pb LA-ICP-MS detrital zircon maximum depositional ages. Dominant detrital zircon peaks represent the Pacific-Gondwana and Grenville clusters common throughout Ordovician and older units of the Tasmanides. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Interleaved with the Greenvale Formation and Wairuna Formation.  Age given as late Cambrian to Early Ordovician.|486 +/- 18 Ma, 495 +/- 6.7 Ma||||Quartzose greywacke with widespread melange and pre-slaty cleavage folding, and uncommon mafic volcanic bodies and chert lenses.|
15032|Pemberton Grange Basalt|35688|2|Defined|p362|early Eocene|Paleocene|Late Paleocene - Early Eocene||||||
15032|Pemberton Grange Basalt|36217|6|Mentioned|p206|||Defined by Robertson 1979.||||||
15032|Pemberton Grange Basalt|36581|6|Mentioned|p462|||||||||
15032|Pemberton Grange Basalt|39445|5|Briefly described|Table 14|||||||||
15032|Pemberton Grange Basalt|39968|6|Mentioned|p75|||||||||
15032|Pemberton Grange Basalt|42895|2|Defined|p53|Early Paleocene|Late Cretaceous|||||||07-NOV-08
15032|Pemberton Grange Basalt|60281|5|Briefly described|p38|||Olivine-rich basalt.  Overlain by Fairymead beds.  Max. thickness: 45m.  Geological Province: Bundaberg Trough (Maryborough Basin).||||||20-JAN-05
15032|Pemberton Grange Basalt|61155|5|Briefly described|p20|Early Eocene|Early Paleocene|Together with Gin Gin Basalt, overlain by Fairymead beds. In the Bundaberg-Maryborough region.||||||
15032|Pemberton Grange Basalt|64714|4|Described|p3-4 Fig. 1, p10-20|Oligocene|Oligocene|Disconformably overlain by Fairymead beds. Age: 24.4+/-0.5Ma, 25+/-2Ma Ar/Ar. Geological province: Bundaberg Trough. Medium-dark grey aphyric and massive to vesicular oliovine basalt, olivine and quartz tholeiite. See also p61, p67 Appdx.||||||26-MAR-15
15032|Pemberton Grange Basalt|68332|5|Briefly described|Map legend.|Oligocene|Oligocene|Bundaberg Volcanic Province. Bundaberg Trough.|25 +/- 2 and 24.4 +/- 0.5 Ma Ar/Ar.||||Medium-dark grey aphyric and massive to amygdaloidal olivine basalt, olivine and quartz tholeiite.|26-MAR-15
15032|Pemberton Grange Basalt|69599|5|Briefly described|p587, p645|Oligocene|Oligocene|Capricorn Basin (onshore). Up to 45m thick in the subsurface. Comprises 5 flows, some separated by weathering and erosional surfaces; the upper surface is deeply weathered. These ages, by Cohen and Vasconcelos (2007), are of the oldest and second youngest flows respectively.|25 +/- 2 Ma to 24.4 +/- 0.5 Ma (40Ar/39Ar).|||Unconformably overlies the Burrum Coal Measures. Is overlain disconformably by Fairymead beds.||
15038|Peninsula Range Volcanics|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15038|Peninsula Range Volcanics|31659|2|Defined|p71|Cretaceous|Permian|Age is Permian or Cretaceous. max. thickness: ~1500ft. Rhyodacitic crystal tuff, rhyolite flows, agglomerate. See also Table 1.||||||08-OCT-08
15038|Peninsula Range Volcanics|32357|4|Described|Table 1|||||||||
15038|Peninsula Range Volcanics|32361|6|Mentioned|Map legend|Cretaceous|Permian|Perm. or Cret.||||||
15038|Peninsula Range Volcanics|38143|6|Mentioned|p13|||||||||
15038|Peninsula Range Volcanics|39445|5|Briefly described|Table 11|||||||||
15038|Peninsula Range Volcanics|41246|6|Mentioned|Map legend|Cretaceous|Permian|||||||
15038|Peninsula Range Volcanics|42660|4|Described|p23 p168|||||||||
15038|Peninsula Range Volcanics|45107|6|Mentioned|p6|||||||||
15038|Peninsula Range Volcanics|61035|5|Briefly described|p18|||Unconformably underlain by Shoalwater Formation. Consists mainly of rhyolitic ignimbrite and lava flows. Geological Province: Coastal Block.||||||07-FEB-11
15038|Peninsula Range Volcanics|68553|6|Mentioned|Map legend|Permian|Permian|This unit, with Double Mountain Volcanics and Berserker Group, are all mapped under the symbol, Pk.||||||
15038|Peninsula Range Volcanics|68679|6|Mentioned|p312-313, p347|Permian|Permian|Northern New England Orogen.||||||
15038|Peninsula Range Volcanics|69952|6|Mentioned|p75|Permian|Permian|||||||
15038|Peninsula Range Volcanics|73197|6|Mentioned|p474-475|Lopingian|Guadalupian|New England Orogen, northern. Coeval with Owl Gully Volcanics, Rookwood Volcanics, Berserker Group, Double Mountain Volcanics.|||||Lavas and pyroclastics.|
15048|Pepper Pot Sandstone|12575|6|Mentioned|p781. |Middle Triassic|Early Triassic|Relatively undeformed.||||||
15048|Pepper Pot Sandstone|23422|5|Briefly described|Plate 7.3|Permian|Early Carboniferous|||||||
15048|Pepper Pot Sandstone|23423|4|Described|p259||Triassic|||||||
15048|Pepper Pot Sandstone|23430|5|Briefly described|p516|||Underlain by Mount Mulligan Coal Measures. In the Ngarrabullan Basin Province.||||||19-FEB-07
15048|Pepper Pot Sandstone|24086|5|Briefly described|p312 Fig. 1|Middle Triassic|Late Permian|||||||
15048|Pepper Pot Sandstone|24213|5|Briefly described|p776 Fig. 1|Middle Triassic|Late Permian|||||||
15048|Pepper Pot Sandstone|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
15048|Pepper Pot Sandstone|31832|6|Mentioned|Table 6|||||||||
15048|Pepper Pot Sandstone|37098|6|Mentioned|p253|||||||||
15048|Pepper Pot Sandstone|37575|6|Mentioned|p179|||||||||
15048|Pepper Pot Sandstone|39445|5|Briefly described|Table 9|||||||||
15048|Pepper Pot Sandstone|42681|4|Described|p22|||||||||
15048|Pepper Pot Sandstone|43285|5|Briefly described|Map Legend||Triassic|||||||
15048|Pepper Pot Sandstone|43625|4|Described|p37,47|||||||||
15048|Pepper Pot Sandstone|43626|6|Mentioned|p15|Triassic|Late Permian|||||||
15048|Pepper Pot Sandstone|43896|14|Not recorded|Map Legend||Triassic|||||||
15048|Pepper Pot Sandstone|43898|14|Not recorded|Map Legend||Triassic|||||||
15048|Pepper Pot Sandstone|44425|14|Not recorded|p14,15,17,19,opp.11,|||Map. Fossils. Terrestrial; with Taeniopteris, Odontopteris, Phyllotheca and Ginkgo present.||||||
15048|Pepper Pot Sandstone|45025|2|Defined|p93-94||Triassic|||||||
15048|Pepper Pot Sandstone|50316|5|Briefly described|Map Legend|Early Triassic|Late Permian|Geological Province: Ngarrabullgan Basin.||||||
15048|Pepper Pot Sandstone|60425|3|Fully described|p5, p14 Tb. 1, p108-9|Middle Triassic|Early Triassic|Has 2 informal subunits. Overlies Mount Mulligan C.M; unconformable on Hodgkinson Formation. Max. thickness: ~800m. Fluvial deposits of mainly lithofeldspathic to quartzose sandstone - detailed lithology included; plant fossils present.||||||07-FEB-11
15048|Pepper Pot Sandstone|62523|4|Described|p17-18, p3-4 (map/legend)|Eary Triassic|Early Triassic|Two unnamed subunits; lower clast-supported rudite, subsid.arenite; upper med- to coarse-gr., granule to pebble-bearing, variably lithic, feldspathic sst. Overlies Mt Mulligan C.M; unconformably overlies Hodgkinson Fm. Max.thick: 800m.||||||07-FEB-11
15048|Pepper Pot Sandstone|64665|5|Briefly described|p53 Fig.2, p56.|Early Triassic|Early Triassic|Ngarrabullan Basin. Written as Pepperpot Sandstone on p53.||||Overlies Mount Mulligan Coal Measures.|Conglomerate and sandstone succession.|
15048|Pepper Pot Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Ngarrabullgan Basin.||||||
15048|Pepper Pot Sandstone|69030|6|Mentioned|p6|Triassic|Triassic|Chillagoe Subprovince, Hodgkinson Province.||||||
15048|Pepper Pot Sandstone|69592|5|Briefly described|p243-244|Middle Triassic|Permian|Ngarrabullgan Basin. Forms cliffs defining the spectacular monolith of Ngarrabullgan (Mount Mulligan). ~300m thick. Conglomerate clasts are derived mainly from Hodgkinson Formation; rhyolite clasts from the adjacent Featherbed Volcanic Group. Fluviatile deposits.||||Overlies Mount Mulligan Coal Measures conformably (locally unconformably). Is overlain by Kondaparinga Formation.|Medium- to coarse-grained, medium- to very thick-bedded lithofeldspathic to quartzose sandstone; subordinate conglomerate (unsorted, sub- to well-rounded clasts) and pebbly sandstone. Sandstones are characteristically red due to hematitic cement.|
15048|Pepper Pot Sandstone|70207|6|Mentioned|p74|Triassic|Triassic|||||||
15048|Pepper Pot Sandstone|70345|6|Mentioned|p3|Triassic|Triassic|||||||
15048|Pepper Pot Sandstone|70673|6|Mentioned|p7|Triassic|Triassic|||||||
15048|Pepper Pot Sandstone|72983|6|Mentioned|p15|Triassic|Triassic|||||||
15060|Percy Creek Volcanics|23422|5|Briefly described|p180, p205 Table 6.3|Carboniferous|Early Carboniferous|Of Glenrock Group. See also Percy Creek volcanics.||||||
15060|Percy Creek Volcanics|23430|5|Briefly described|p506|||Of Glenrock Group. Overlain by Mount Douglas Formation. Burdekin Basin Province.||||||23-APR-08
15060|Percy Creek Volcanics|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Glenrock Group.||||||23-APR-08
15060|Percy Creek Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V47.||||||
15060|Percy Creek Volcanics|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
15060|Percy Creek Volcanics|24334|5|Briefly described|p48 Tb.1|Namurian|Tournaisian|Age: 317 - 345 Ma.||||||23-APR-08
15060|Percy Creek Volcanics|24613|2|Defined|p9 Fig. 4, p92, p94-95|Visean|Visean|Now included in Glenrock Gp. Conformable below Mount Douglas Fm. Intruded by Emysland Granodiorite + Boolangalla Granophyre. Thick: 600m (est). Geol.prov: Burdekin Basin. Dominant lith.is andesite + subsid'y basalt, basaltic andesite - lith.details incl.||||||07-FEB-11
15060|Percy Creek Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
15060|Percy Creek Volcanics|32169|6|Mentioned|Table 2|||U.Carb.||||||
15060|Percy Creek Volcanics|32553|4|Described|p44|||||||||
15060|Percy Creek Volcanics|33871|6|Mentioned|Table 4|||||||||
15060|Percy Creek Volcanics|34408|6|Mentioned|p185|||On table||||||
15060|Percy Creek Volcanics|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
15060|Percy Creek Volcanics|37573|4|Described|p225|||||||||
15060|Percy Creek Volcanics|37613|6|Mentioned|p249|||See also Fig.3||||||
15060|Percy Creek Volcanics|39445|5|Briefly described|Table 7|||||||||
15060|Percy Creek Volcanics|39686|6|Mentioned|p73|||||||||
15060|Percy Creek Volcanics|39735|6|Mentioned|p18|||||||||
15060|Percy Creek Volcanics|40607|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
15060|Percy Creek Volcanics|42547|5|Briefly described|p76|||||||||
15060|Percy Creek Volcanics|42689|5|Briefly described|map legend|Carboniferous||||||||
15060|Percy Creek Volcanics|43095|5|Briefly described|Plate 1|||Of Glenrock Group.||||||23-APR-08
15060|Percy Creek Volcanics|43259|4|Described|Appendix 1,p5.||Early Carboniferous|Of Glenrock Group.||||||23-APR-08
15060|Percy Creek Volcanics|43589|6|Mentioned|p18||Early Carboniferous|Possibly an equivalent to Taralee Volcanics.  On the TOWNSVILLE 1:250K sheet area.||||||23-APR-08
15060|Percy Creek Volcanics|43933|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||
15060|Percy Creek Volcanics|43935|5|Briefly described|Map Legend||Carboniferous|Of Glenrock Group.||||||22-FEB-05
15060|Percy Creek Volcanics|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
15060|Percy Creek Volcanics|44061|4|Described|Table 3||Late Carboniferous|||||||
15060|Percy Creek Volcanics|44790|14|Not recorded|p441|||Late Middle Upper Carboniferous||||||
15060|Percy Creek Volcanics|45151|5|Briefly described|Table 7|||||||||
15060|Percy Creek Volcanics|46845|6|Mentioned|Table 1|||||||||
15060|Percy Creek Volcanics|48904|4|Described|p36|||U.Carb.||||||
15060|Percy Creek Volcanics|68731|5|Briefly described|p187|||< 600 m thick.||||Unconformably underlain by the Keelbottom Group.|Comprises largely pyroxene-bearing, massive to amygdaloidal, porphyritic andesite flows. Subordinate basalt and basaltic andesite and rare volcanic breccia are represented in the succession.|
15063|Percy Granophyre|23446|5|Briefly described|p447|||In Coolgarra Batholith.||||||
15063|Percy Granophyre|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 314 +/- 3 Ma, Rb-Sr.||||||
15063|Percy Granophyre|23506|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 314+/-3Ma Rb-Sr.||||||
15063|Percy Granophyre|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 260. I-Type.||||||
15063|Percy Granophyre|23616|6|Mentioned|Table 6 p73|||Of O'Briens Creek Supersuite.||||||
15063|Percy Granophyre|40743|6|Mentioned|p311|||||||||
15063|Percy Granophyre|41297|6|Mentioned|Fig.1|||||||||
15063|Percy Granophyre|42200|6|Mentioned|p325|||||||||
15063|Percy Granophyre|43060|5|Briefly described|Table 6|||of O'Briens Creek Supersuite||||||
15063|Percy Granophyre|43259|4|Described|Appendix 1,p34.||Carboniferous|||||||
15063|Percy Granophyre|60425|4|Described|p282-3 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Ages: 314Ma, 313+/-13Ma, 314+/-3Ma, 315+/-10Ma (Rb-Sr). Pink to cream to pale yellow, fine-grained, granophyric biotite granite.  I-type.||||||07-FEB-11
15066|Peringa Tonalite|22780|5|Briefly described|map|Early Devonian|Late Silurian|Flyspeck Supersuite||||||
15066|Peringa Tonalite|22781|4|Described|p26|Paleozoic|Paleozoic|Flyspeck Supersuite||||||07-NOV-08
15066|Peringa Tonalite|23420|4|Described|p 148 table 4.7||Early Devonian|In the Flyspeck Supersuite. Intruded by Bunira Granite||||||
15066|Peringa Tonalite|42610|2|Defined|p23|Early Devonian|Early Devonian|Age ass. sim. Glen Garland Gran., 398Ma. Prev. incl. in "Kintore Adamellite. Res. as P Granodiorite.||||||
15066|Peringa Tonalite|43596|6|Mentioned|p36|||Of Mackenzie et al 1992; Mackenzie and Knutson 1992).  Now incorporated into the Bunira Granite, was formerly the northern part of it.||||||27-JAN-09
15066|Peringa Tonalite|43738|6|Mentioned|Fig.12,p38|||||||||
15066|Peringa Tonalite|69592|6|Mentioned|p282|||Cape York Peninsula Batholith.||Flyspeck Supersuite.||||
15073|Perry Creek Formation|23032|4|Described|p19||Early Silurian|||||||
15073|Perry Creek Formation|23422|5|Briefly described|p175|Silurian|Silurian|||||||
15073|Perry Creek Formation|23423|5|Briefly described|Plate 8.2c|||||||||
15073|Perry Creek Formation|23424|4|Described|Table 8.1 Fig 8.2 p333.|Early Silurian|Late Ordovician|Age determined with corals & conodonts in allochthonous limestone. Faulted against Pelican Range Fm and Kangaroo Hills Fm. Overlying unit Clarke River Group (u). Camel Creek Subprovince. Max. thickness 350 m.||||||
15073|Perry Creek Formation|23430|5|Briefly described|p476|||Broken River Province.||||||
15073|Perry Creek Formation|23431|5|Briefly described|p538|||||||||
15073|Perry Creek Formation|23494|4|Described|p9, p21 Tb. 1|Early Devonian|Late Silurian|Limestone reef succession. Conformably overlies Kangaroo Hills Formation.  Max. thickness: 3500ft.||||||23-APR-08
15073|Perry Creek Formation|23498|5|Briefly described|p22  table 1|Early Devonian|Late Silurian|Conformably overlies Kangaroo Hills Formation||||||
15073|Perry Creek Formation|23509|5|Briefly described|Map Legend|Early Devonian|Ordovician|of Broken River Province.||||||
15073|Perry Creek Formation|23617|5|Briefly described|p13 + 22||Silurian|Camel Creek Subprovince Broken Hill Province.||||||
15073|Perry Creek Formation|23619|4|Described|p34 Table 1||Silurian|Contains strongly cleaved turbidites. Also see p8. Age based on coral and conodonts from limestone lenses. Broken River Province.||||||
15073|Perry Creek Formation|23893|5|Briefly described|p14|Early Silurian|Early Silurian|Intruded by Kallanda Granite.  Geological Province: Camel Creek Subprovince.||||||
15073|Perry Creek Formation|24074|5|Briefly described|p389 Table 1|Late Silurian|Late Silurian|Maximum thickness: 1000m.||||||
15073|Perry Creek Formation|24577|4|Described|p752 Fig. 1|Silurian|Silurian|Overlain? by the Kangaroo Hills Formation. Overlies the Greenvale Formation. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||23-APR-08
15073|Perry Creek Formation|24613|5|Briefly described|p92|Silurian|Silurian|Unconformably overlain by Ewan Formation, which is partly faulted against both Running River Metamorphics and this unit. Underlies Burdekin Basin in the Ewan area.||||||07-FEB-11
15073|Perry Creek Formation|29445|6|Mentioned|p73|||||||||
15073|Perry Creek Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Ordovician - Devonian||||||
15073|Perry Creek Formation|31832|6|Mentioned|Table 6|||||||||
15073|Perry Creek Formation|31999|6|Mentioned|p137|||Table 11||||||
15073|Perry Creek Formation|32553|4|Described|p52|||||||||
15073|Perry Creek Formation|34252|6|Mentioned|Ps.2|||Fossils||||||
15073|Perry Creek Formation|35008|6|Mentioned|p179|||||||||
15073|Perry Creek Formation|37573|4|Described|p202|||||||||
15073|Perry Creek Formation|37575|4|Described|p181|||See also Fig.3||||||
15073|Perry Creek Formation|37727|4|Described|p81|||See also p22.||||||23-APR-08
15073|Perry Creek Formation|39027|6|Mentioned|Map legend|Early Devonian|Late Silurian|Upper Silurian to Lower Devonian||||||
15073|Perry Creek Formation|39445|5|Briefly described|Table 5|||See also P64, P74 & Fig.6. Devonian corals. Exotic blocks||||||
15073|Perry Creek Formation|39686|6|Mentioned|Fig.1|||||||||
15073|Perry Creek Formation|39689|6|Mentioned|p52|||||||||
15073|Perry Creek Formation|39987|6|Mentioned|p66|||||||||
15073|Perry Creek Formation|40623|5|Briefly described|p92|||||||||
15073|Perry Creek Formation|40787|5|Briefly described|p331|||||||||
15073|Perry Creek Formation|40943|6|Mentioned|p50|||||||||
15073|Perry Creek Formation|41260|3|Fully described|p16|||Described p116 and p136.||||||23-APR-08
15073|Perry Creek Formation|41916|4|Described|p28|||||||||
15073|Perry Creek Formation|42031|6|Mentioned|Fig.6 P763|||||||||
15073|Perry Creek Formation|42279|6|Mentioned|p28|||||||||
15073|Perry Creek Formation|42407|6|Mentioned|p26|||||||||
15073|Perry Creek Formation|42690|5|Briefly described|map legend|Early Devonian|Ordovician?|||||||
15073|Perry Creek Formation|42692|5|Briefly described|map legend|Early Devonian|Silurian|||||||
15073|Perry Creek Formation|42752|5|Briefly described|p45|||see also Fig.2 P46||||||
15073|Perry Creek Formation|42933|2|Defined|p25|Early Devonian|Silurian|||||||
15073|Perry Creek Formation|43095|5|Briefly described|Plate 2.|||||||||
15073|Perry Creek Formation|43113|4|Described|Table 1 p20||Silurian|||||||
15073|Perry Creek Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
15073|Perry Creek Formation|43259|6|Mentioned|Appendix 1,p4.|Silurian|Late Ordovician|||||||
15073|Perry Creek Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
15073|Perry Creek Formation|43589|6|Mentioned|p22, p23||Silurian|Forms a septum between two bodies of granite of the Kallanda Granite batholith.||||||23-APR-08
15073|Perry Creek Formation|43902|14|Not recorded|p119|||||||||
15073|Perry Creek Formation|44044|14|Not recorded|p124-127|||Conformably overlies Kangaroo Hills Formation. Part=Graveyard Creek Formation.||||||
15073|Perry Creek Formation|44046|14|Not recorded|p149|||||||||
15073|Perry Creek Formation|44059|14|Not recorded|p442(Tb)|Early Devonian|Late Silurian|||||||
15073|Perry Creek Formation|44080|14|Not recorded|Tb.A, p151|||||||||
15073|Perry Creek Formation|44515|2|Defined|p34-36|Early Devonian|Late Silurian|Overlain by Clarke River Formation. Similar in age to Jack Limestone. Grades into Tribute Hill Sandstone.||||||
15073|Perry Creek Formation|44516|14|Not recorded|p35|||||||||
15073|Perry Creek Formation|45009|2|Defined|p7,46,48,50-2,61,|||Pl.13,Tb.5,6. Grades into Tribute Hill Sandstone.||||||23-APR-08
15073|Perry Creek Formation|45151|6|Mentioned|p7|||||||||
15073|Perry Creek Formation|48904|6|Mentioned|p16|||||||||
15073|Perry Creek Formation|61727|5|Briefly described|p942 Fig.1|Devonian|Silurian|Geological Province: Broken River Province/Camel Creek Subprovince.||||||
15073|Perry Creek Formation|61894|6|Mentioned|p189|Silurian|Silurian|Pseudoplasmopora follis (photographs of sections) occurs in this unit.||||||
15073|Perry Creek Formation|63154|5|Briefly described|p281 Fig. 3|Silurian|Silurian|Geological province: Broken River Province/Camel Creek Subprovince.||||||
15073|Perry Creek Formation|67848|5|Briefly described|p3 Fig.2, p8.|||Camel Creek Subprovince. Part of the accretionary wedge in the arc-trench gap succession involved in collisional accretion. Contains allochthonous limestone clasts and blocks, with late Ordovician to mid-Silurian conodonts, interpreted as being from Carriers Well Formation.||||||
15073|Perry Creek Formation|68339|5|Briefly described|Map legend.|Silurian|Silurian|Camel Creek Subprovince.|||||Lithofeldspathic sublabile to labile arenite, mudstone and grey chert, local melange; large limestone lenses, probably allochthonous; grey to green bedded chert; altered aphyric tholeiitic basalt, locally pillowed, chert and jasper.|14-APR-15
15073|Perry Creek Formation|68340|5|Briefly described|Map legend.|Silurian|Silurian|Camel Creek Subprovince.|||||Lithofeldspathic sublabile to labile arenite, mudstone and grey chert, local melange; large limestone lenses, probably allochthonous; grey to green bedded chert; altered aphyric tholeiitic basalt, locally pillowed, chert and jasper.|
15073|Perry Creek Formation|68350|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince, Broken River Province. Age min: Early Devonian?|||||Lithofeldspathic sublabile to labile arenite, mudstone and grey chert, local melange; sheared and recrystallised limestone including skarn is mapped separately.|07-JUL-15
15073|Perry Creek Formation|68351|5|Briefly described|Map legend.||Late Ordovician?|Camel Creek Subprovince, Broken River Province. Age min: Early Devonian?|||||Lithofeldspathic sublabile to labile arenite, mudstone and grey chert, local melange; sheared and recrystallised limestone including skarn is mapped separately.|07-JUL-15
15073|Perry Creek Formation|68480|5|Briefly described|Map Legend|Silurian|Silurian|Camel Creek Subprovince. The 3 facies are mapped separately.|||||Undivided: lithofeldspathic sublabile to labile arenite, mudstone and grey chert; local melange. Separately mapped are: jasper; altered aphyric tholeiitic basalt, locally pillowed, chert and jasper.|
15073|Perry Creek Formation|68481|5|Briefly described|Map Legend|Silurian|Silurian|Camel Creek Subprovince. The 3 facies are mapped separately.|||||Undivided: lithofeldspathic sublabile to labile arenite, mudstone and grey chert; local melange. Separately mapped are: jasper; altered aphyric tholeiitic basalt, locally pillowed, chert and jasper.|
15073|Perry Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Broken River Province. This unit, as well as Greenvale and Kangaroo Hills Formations, are all mapped under the symbol, SDb.||||||
15073|Perry Creek Formation|68576|5|Briefly described|Q_11: p38-40|||Camel Creek Subprovince. Crops out as bluffs. Interpreted as olistostromes. Locally quarried for aggregate. Contains Silurian conodonts and Halysites. Source of clasts for an unnamed conglomerate in the basal Clarke River Group.|||||Limestone.|
15073|Perry Creek Formation|68731|6|Mentioned|p187|||Broken River Province.||||Unconformably overlain by the Ewan Formation.||
15073|Perry Creek Formation|69030|6|Mentioned|p6|Silurian|Silurian|Camel Creek Subprovince (Broken River Province).||||||
15073|Perry Creek Formation|69079|6|Mentioned|p5, p65|Early Devonian|Silurian|Camel Creek Subprovince, Broken River Province. Hosts small gold prospects in NNE-striking faults in the Mount Picklebottle area.||||||
15073|Perry Creek Formation|69592|5|Briefly described|p251 Fig.4.35, p260, p269 Fig.4.56|Late Silurian|Late Silurian|See also p270-272, p278-279, p297, p303. Camel Creek Subprovince, Broken River Province. A continuous topographically prominent belt; contacts presumed to be faulted. Contains limestone olistolith bodies transported downslope from an unstable shallow-marine shelf; similar to Crooked Creek Conglomerate in Graveyard Creek Subprovince. Lenses of aphyric basalt, up to 15km long and 1500m thick; locally pillowed, with hyaloclastic breccia zones. Geochemical plots.||||Is faulted against Kangaroo Hills Formation.|Intervals of thick- to very thick-bedded, medium- to coarse-grained sandstone alternating with mudstone, commonly laminated; sporadic bodies of chert (up to 56m thick) and limestone and lenses of cobble (sporadically boulder) conglomerate.|
15073|Perry Creek Formation|70207|6|Mentioned|p20|Early Devonian|Silurian|Clarke River and/or Cairns region.||||||
15073|Perry Creek Formation|73201|4|Described|p607, p610-618, p620|Middle Devonian|Silurian|Broken River Province. Geochron is a U-Pb LA-ICP-MS detrital zircon maximum depositional age. Unit is likely to be Devonian, but its age is not closely constrained. Characterised by scattered blocks and lenses of limestone (interpreted as olistoliths) that contain Late Ordovician to mid-Silurian fossils. Detrital zircon provenance is linked to igneous rocks of the Macrossan and Pama Igneous associations. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Age given as late Silurian to Middle Devonian.|388 +/- 13 Ma||||Lithofeldspathic greywacke with widespread melange and pre-slaty cleavage folding, and common mafic volcanic bodies, chert lenses, polymict conglomerate horizons, and limestone olistoliths.|
15073|Perry Creek Formation|73425|6|Mentioned|p3||||||||Arenites, chert, limestone.|
15114|Peters Creek Volcanics|22457|4|Described|P29, Fig29, Fig30|||Shown as Upper and Lower Peters Creek Volcanics Fig29 p30.||||||22-NOV-06
15114|Peters Creek Volcanics|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
15114|Peters Creek Volcanics|22644|6|Mentioned|5 fig 2|||Geol province Mount Isa Basin. Volcanics as 'V' in text||||||
15114|Peters Creek Volcanics|22665|5|Briefly described|P221, Table1|Statherian|Statherian|Ages of unit are 1726+/-2 Ma (lower) and 1724+/-2 Ma (upper)||||||
15114|Peters Creek Volcanics|22673|6|Mentioned|64,65,79|||Geol province Mount Isa Basin. Overlying unit Fickling Group||||||
15114|Peters Creek Volcanics|22680|6|Mentioned|85|||||||||
15114|Peters Creek Volcanics|23065|6|Mentioned|16|Proterozoic|Proterozoic|Geol province Lawn Hill Subprovince. Age ~1725 Ma. Underlying unit is Wire Creek Sandstone.||||||21-FEB-18
15114|Peters Creek Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
15114|Peters Creek Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15114|Peters Creek Volcanics|23395|4|Described|p384 Fig.2|||||||||
15114|Peters Creek Volcanics|23396|4|Described|p415|||||||||
15114|Peters Creek Volcanics|23397|5|Briefly described|p466|||||||||
15114|Peters Creek Volcanics|23398|4|Described|p437|Statherian|Statherian|U/Pb SHRIMP pooled age: 1729+/-4Ma.||||||09-SEP-14
15114|Peters Creek Volcanics|23406|5|Briefly described|p601 Fig. 3, p603, p604 Fig. 6|||Age: 1730-1710Ma. Stated to be of a basal "rift" package. Forms an igneous dome. Parts contained as clasts in the Fish River Formation. Thickest at Hedleys Creek.  See also p600 Fig. 2.||||||16-JUN-09
15114|Peters Creek Volcanics|23409|5|Briefly described|p535|||Of Lawn Hill Platform.||||||11-JUN-08
15114|Peters Creek Volcanics|24197|5|Briefly described|p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1710Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1. See also the possibly misspelt Peter Creek Volcanics (although both names may be in use?)||||||07-FEB-11
15114|Peters Creek Volcanics|24308|5|Briefly described|p998, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15114|Peters Creek Volcanics|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
15114|Peters Creek Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1725+/-3 Ma. Geological Province: Lawn Hill Platform.||||||28-JAN-05
15114|Peters Creek Volcanics|26310|5|Briefly described|p7 Fig. 2, Table 1.|Neoproterozoic|Neoproterozoic|Acidic to basic, generally intermediate lavas, with interbedded sediments.||||||09-AUG-04
15114|Peters Creek Volcanics|29966|6|Mentioned|p398|||||||||
15114|Peters Creek Volcanics|30318|6|Mentioned|p328|||||||||
15114|Peters Creek Volcanics|31348|6|Mentioned|p344|||||||||
15114|Peters Creek Volcanics|31421|6|Mentioned|p509|||||||||
15114|Peters Creek Volcanics|32660|5|Briefly described|Table 4|||||||||
15114|Peters Creek Volcanics|33214|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|35114|6|Mentioned|p200|||||||||
15114|Peters Creek Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|36012|3|Fully described|Table 3|||See also p11,16.||||||22-NOV-06
15114|Peters Creek Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15114|Peters Creek Volcanics|37462|4|Described|Table4.VII|||||||||
15114|Peters Creek Volcanics|37565|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|37568|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|38237|6|Mentioned|p126|||||||||
15114|Peters Creek Volcanics|38557|5|Briefly described|p293|||||||||
15114|Peters Creek Volcanics|38584|4|Described|p15|||||||||
15114|Peters Creek Volcanics|38835|6|Mentioned|p164|||||||||
15114|Peters Creek Volcanics|39445|5|Briefly described|Table 2|||See also P36 & P39||||||
15114|Peters Creek Volcanics|39497|6|Mentioned|p8|||See also Fig.4||||||
15114|Peters Creek Volcanics|39685|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|39925|6|Mentioned|p334|||||||||
15114|Peters Creek Volcanics|39944|6|Mentioned|Fig.5|||||||||
15114|Peters Creek Volcanics|40105|6|Mentioned|p310|||||||||
15114|Peters Creek Volcanics|40491|6|Mentioned|p79|||||||||
15114|Peters Creek Volcanics|40811|6|Mentioned|p318|||||||||
15114|Peters Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
15114|Peters Creek Volcanics|41125|6|Mentioned|Fig.21|||||||||
15114|Peters Creek Volcanics|41319|6|Mentioned|Fig.1|||||||||
15114|Peters Creek Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
15114|Peters Creek Volcanics|41721|3|Fully described|p27|||Originally mapped by Roberts et al (1963). Lower part is replaced by Seigal Volcanics.||||||01-AUG-07
15114|Peters Creek Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
15114|Peters Creek Volcanics|42639|5|Briefly described|p8|||Lawn Hill Platform||||||
15114|Peters Creek Volcanics|42812|6|Mentioned|p65|||||||||
15114|Peters Creek Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
15114|Peters Creek Volcanics|43788|6|Mentioned|p14|||||||||
15114|Peters Creek Volcanics|44271|2|Defined|p39,44,57|||||||||
15114|Peters Creek Volcanics|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
15114|Peters Creek Volcanics|44274|14|Not recorded|p8,Tb.2|||||||||
15114|Peters Creek Volcanics|44275|14|Not recorded|Map Legend|||||||||
15114|Peters Creek Volcanics|44280|2|Defined|p5,Tb.1,map||Neoproterozoic|||||||
15114|Peters Creek Volcanics|44287|14|Not recorded|p.8, opp.7|||(E53-3).||||||
15114|Peters Creek Volcanics|44288|14|Not recorded|map legend||Paleoproterozoic|Amygdoloidal basalt, minor trachyte. Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44305|14|Not recorded|p.6,11,19,20||Neoproterozoic|(E53-8). opp.p.6,18. Includes Carolina Sandstone Member. U.Prot.||||||
15114|Peters Creek Volcanics|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44473|14|Not recorded|p.8, opp. p.7|||(E53-7). Formation of Tawallah Group.||||||
15114|Peters Creek Volcanics|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44530|14|Not recorded|p,4,8, opp.8|||(D53-15).||||||
15114|Peters Creek Volcanics|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
15114|Peters Creek Volcanics|44806|14|Not recorded|p297|||Petrographic description.||||||
15114|Peters Creek Volcanics|44989|2|Defined|p.115-7|||Tb.II. On many pages. Pl.8. Overlies Cliffdale Volcanics, Westmoreland Conglomerate; underlies Wollogorang Formation (E54-5).||||||12-AUG-08
15114|Peters Creek Volcanics|45162|6|Mentioned|p14|||Mention P27||||||
15114|Peters Creek Volcanics|45166|5|Briefly described|p26|||See also P50||||||
15114|Peters Creek Volcanics|45287|14|Not recorded|p.223,226|||||||||
15114|Peters Creek Volcanics|46804|6|Mentioned|p154|||||||||
15114|Peters Creek Volcanics|46919|6|Mentioned|p221|||||||||
15114|Peters Creek Volcanics|48867|14|Not recorded|p.7|||Equivalent to part of Kombolgie Formation.||||||
15114|Peters Creek Volcanics|49001|6|Mentioned|p4|||||||||
15114|Peters Creek Volcanics|49002|6|Mentioned|p1|||||||||
15114|Peters Creek Volcanics|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
15114|Peters Creek Volcanics|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Supersuite. Age: 1724-1726 +/- 2Ma (Shrimp).||||||07-NOV-08
15114|Peters Creek Volcanics|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Age: ~1725Ma.||||||07-NOV-08
15114|Peters Creek Volcanics|60558|6|Mentioned|p5 Fig. 4|||||||||
15114|Peters Creek Volcanics|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1730-1725Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
15114|Peters Creek Volcanics|63109|5|Briefly described|p1109, p1108 Fig. 3|||Overlain by Surprise Creek Formation, underlain by Bigie Formation. Felsic rocks. Geological Province: Murphy Inlier.||||||08-MAR-13
15114|Peters Creek Volcanics|63110|6|Mentioned|p1141, p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
15114|Peters Creek Volcanics|63113|6|Mentioned|p1214 Fig.2, 1225 Fig.13.||||c.1729-1724 Ma.|||Overlies ?unconformably Buddawadda Basalt.||
15114|Peters Creek Volcanics|63115|6|Mentioned|1279 Fig.4, p1281, p1290. |||Calvert superbasin.||||||
15114|Peters Creek Volcanics|63116|6|Mentioned|p1297 Fig.2, |||Calvert superbasin.||||||
15114|Peters Creek Volcanics|63866|5|Briefly described|p56|Statherian|Statherian|Murphy Inlier, Calvert Superbasin. Numeric dates derived from Page and Sweet, 1998 and Page et al., 2000.|1729 +/- 4 Ma and 1724 +/- 2 Ma|||||
15114|Peters Creek Volcanics|64250|6|Mentioned|p11 fig 3, p24, p19|||Of far NW of Mt Isa Inlier. May be intrusive.|1729 +/- 4 Ma - 1725 +/- 2 Ma||||Bimodal volcanics: basalt, rhyolite.|
15114|Peters Creek Volcanics|64575|6|Mentioned|p656|||Geological Province: Murphy Inlier.||||||
15114|Peters Creek Volcanics|64726|6|Mentioned|p86 Table 1.|||Sampled for paleomagnetic reconstruction of Australian and Laurentian Apparent Polar Wander Path.|1724 +/- 2 Ma.|||||
15114|Peters Creek Volcanics|64738|6|Mentioned|pp260-261.|Statherian|Statherian|Dated and used in identifying a right-angle bend in the earliest defined segment of northern Australia's Apparent Polar Wander Path.|c.1730 Ma.|||||
15114|Peters Creek Volcanics|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Basalt. Palaeomag results shown on polar wander path||||||
15114|Peters Creek Volcanics|64817|6|Mentioned|p351 Fig.2|||||||||
15114|Peters Creek Volcanics|65228|5|Briefly described|Figs.04, 07.|Statherian|Statherian|Southern McArthur Basin. Part of the Big Supersequence.|1729 +/- 4 Ma and 1724 +/- 2 Ma.||Includes Buddawarra Basalt.|Overlies Wire Creek Sandstone.||
15114|Peters Creek Volcanics|65337|5|Briefly described|p5. |||Leichhardt Superbasin; Lawn Hill Platform. Correlative of Carrara Range Group.|1729 +/- 4 Ma.||||Includes intrusive rhyodacites.|
15114|Peters Creek Volcanics|65340|6|Mentioned|p35, p93.|||Murphy Inlier. Part-correlated with Settlement Creek Dolerite and Gold Creek Volcanics.||||||
15114|Peters Creek Volcanics|65396|5|Briefly described|p82, p175, p187, p192-193, p195, p197|Statherian|Statherian|See also p241. Calvert Superbasin, far NW of Mount Isa Inlier. Cover Sequence 2. Formations with detrital zircons from this unit are listed.|1729 +/- 4 Ma, 1725 +/- 2 Ma||||Basalt and rhyolite.|
15114|Peters Creek Volcanics|66529|6|Mentioned|p3|||Calvert Superbasin.|~1730-1720 Ma|||||
15114|Peters Creek Volcanics|67323|5|Briefly described|GIS attrib tbl,  p9-10, p33, p107|Statherian|Statherian|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Northern Camooweal-Murphy Domain, Mount Isa Inlier, Calvert Superbasin. Ages: 1729+/-4 Ma, 1724+/-4 Ma (1998, 2000), significantly older than Fiery Creek Volcanics.|1724+/-4 Ma||Includes Buddawadda Basalt Member, and 12 unnamed subdivisions.||Basalt, rhyolite, sandstone and conglomerate.|
15114|Peters Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|McArthur Basin, Mount Isa Province.||||Conformably overlies Tawallah Group.||
15114|Peters Creek Volcanics|68575|6|Mentioned|p11|||||||Is overlain by Fickling Group.||
15114|Peters Creek Volcanics|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
15114|Peters Creek Volcanics|69430|6|Mentioned|p15:1|||||||||12-JUL-16
15114|Peters Creek Volcanics|69433|4|Described|p18:1-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Exposed in SW corner of CALVERT HILLS map area, but more completely in Qld. Forming a 10x50km belt. Geochemically distinct from Buddycurrawa Volcanics. The basalts in the lower part of the unit are probably equivalent to Seigal Volcanics. SHRIMP U-Pb zircon ages (Page and Sweet, 1998).|1726 +/- 2 Ma and 1724 +/- 2 Ma.|||Overlies probably conformably Wire Creek Sandstone. Is overlain unconformably by Fish River Formation (Fickling Group). Equivalent to upper Tawallah Group (McArthur Basin) and Carrara Range Group.|Vesicular and massive basaltic lavas with fine to medium sandstone interbeds; rhyolite, rhyodacite, tuff, shale, siltstone, dolostone and conglomerate.|12-JUL-16
15114|Peters Creek Volcanics|69591|4|Described|p29, p34, p38, p56, p106|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Calvert Superbasin. Part of the Big Supersequence. Mostly high-level intrusives, with chemical and lithological similarities to Packsaddle Microgranite; also, sedimentary units (shallow-marine) have similarities to the Wollogorang Formation.|1726 +/- 2 Ma (Page and Sweet, 1998).||Buddawadda Basalt Member.|Is overlain by the Bigie Formation.|Basalt, rhyolite, sandstone, conglomerate.|
15114|Peters Creek Volcanics|69673|5|Briefly described|p51|Statherian|Statherian|Considered to be equivalent to the Tawallah Group of the McArthur Basin. Total thickness of 2km.|1726 +/- 2 Ma|||Unconformably overlain by Fickling Group|Vesicular and massive basaltic lavas with sandstone interbeds.|
15114|Peters Creek Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Tawallah Group equivalent.||Overlies Wire Creek Sandstone. Is overlain unconformably by Fish River Formation (Fickling Group).|Alternating sequence of basalt, rhyolite and rhyodacite; some intermediate volcanics, possibly trachyte and andesite; minor tuff, shale, siltstone, sandstone, dolomite and conglomerate.|21-FEB-18
15114|Peters Creek Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1726+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite, rhyolite.|
15114|Peters Creek Volcanics|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain unconformably by Fickling Group. Underlain by Wire Creek Sandstone.||
15114|Peters Creek Volcanics|71632|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|Shown elsewhere in map key as Lower Peters Creek Volcanics and Upper Peters Creek Volcanics. Unit evidently expanded in this map to include Wire Creek Sandstone, but this change appears to be a one off, not used again].||||||
15114|Peters Creek Volcanics|71799|5|Briefly described|p150 fig 2, p153 tbl 1|Statherian|Statherian|McArthur Basin. Age is derived from SHRIMP U-Pb magmatic ages (not provided) derived from Page et al, 2000 and from Page, 1983. Geochemistry is discussed. See also p154, p156, p157 fig 5, p158.|1730-1720 Ma||||Basalt, dolerite, gabbro or amphibolite.|
15114|Peters Creek Volcanics|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|U-Pb SHRIMP igneous crystallisation ages given. Shown as being located in the west of the South Nicholson Basin.|1725+/-2 Ma, 1729+/-4 Ma|||Overlies Wire Creek Sandstone and shown as partially underlying Benmara Group and Fickling Group.||
15114|Peters Creek Volcanics|72527|4|Described|p2, p7 Fig.1.4, p9, p87, p89, p176-177.|Paleoproterozoic|Paleoproterozoic|Insufficient zircon yield to enable meaningful date results. One of three units considered to represent c. 1725 Ma felsic volcanism in the region, including Top Rocky Rhyolite and Hobblechain Volcanics. See also p192, p194 and p196.|c. 1725 Ma (Page et al., 2000)|Tawallah Group||Unconformably overlies Wire Creek Sandstone and is laterally equivalent to Top Rocky Rhyolite.||
15114|Peters Creek Volcanics|72912|5|Briefly described|p5 Fig.3, p13, p17.|Statherian|Statherian|Calvert Superbasin. Located in the west part of the South Nicholson Basin. Three U-Pb zircon igneous crystallisation ages (Ma) shown.|1729 +/- 4 Ma to 1725 +/- 2 Ma||||Bimodal volcanics.|
15114|Peters Creek Volcanics|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1729+/-4 Ma, 1726+/-2 Ma, 1725+/-2 Ma|||||
15114|Peters Creek Volcanics|73083|6|Mentioned|p77|||||||||
15114|Peters Creek Volcanics|73412|6|Mentioned|p20|||Western Succession of the Mount Isa Inlier. Contains potassic alteration assemblages, interpreted as regional fluid flow associated with Zn-Pb-Ag metallogenesis.||||||
15114|Peters Creek Volcanics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
15129|Petrie Formation|24160|6|Mentioned|p18|||Brisbane area; hosts bentonite deposits.||||||
15129|Petrie Formation|30797|5|Briefly described|Table 1|||Tertiary, particulary useful as source of ceramic materials.||||||
15129|Petrie Formation|32883|6|Mentioned|p47|||||||||
15129|Petrie Formation|33368|6|Mentioned|p48|||Palaeoc.-Olig.||||||
15129|Petrie Formation|33881|5|Briefly described|p96|||||||||
15129|Petrie Formation|35053|6|Mentioned|p36|||||||||
15129|Petrie Formation|35430|6|Mentioned|Fig.2|||Geological map.||||||
15129|Petrie Formation|36238|6|Mentioned|Table 1|||||||||
15129|Petrie Formation|36440|6|Mentioned|Map legend|Eocene|Paleocene|Eocene to Palaeocene||||||
15129|Petrie Formation|36547|6|Mentioned|Table 2|||||||||
15129|Petrie Formation|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15129|Petrie Formation|38074|5|Briefly described|Table 1|||||||||
15129|Petrie Formation|39079|5|Briefly described|p10|||||||||
15129|Petrie Formation|39445|5|Briefly described|p153|||Clay deposits. See also Table 14||||||
15129|Petrie Formation|40579|6|Mentioned|Map legend|Eocene|Eocene|||||||
15129|Petrie Formation|40623|5|Briefly described|p8|||||||||
15129|Petrie Formation|40723|5|Briefly described|p260|||||||||
15129|Petrie Formation|42316|5|Briefly described|p18|||||||||
15129|Petrie Formation|42525|5|Briefly described|Map legend|Miocene|Paleocene|||||||
15129|Petrie Formation|43076|5|Briefly described|p11|||||||||
15129|Petrie Formation|43895|4|Described|p114,115|||Ceramic materials.||||||
15129|Petrie Formation|44128|14|Not recorded|Tb.1,p426|||||||||
15129|Petrie Formation|44430|14|Not recorded|p266,Fig.37||Tertiary|||||||
15129|Petrie Formation|44581|14|Not recorded|p353||Oligocene|||||||
15129|Petrie Formation|44677|14|Not recorded|p1|||||||||
15129|Petrie Formation|44687|1|Redefined|p226-227|||See also Lexicon.||||||
15129|Petrie Formation|44703|14|Not recorded|Map|||||||||
15129|Petrie Formation|44704|14|Not recorded|p1,4,9|||||||||
15129|Petrie Formation|44708|14|Not recorded|p3,5,23,Sh.3,5,sect||Tertiary|||||||
15129|Petrie Formation|44710|14|Not recorded|p453||Tertiary|||||||
15129|Petrie Formation|44783|14|Not recorded|p2,Tb.1,p11|||||||||
15129|Petrie Formation|44786|14|Not recorded|p193-202||Oligocene|||||||
15129|Petrie Formation|44911|14|Not recorded|p4|||Probably equivalent 2 formations, and name will probably be revised. Clay ironstone, sandstone & boulder conglomerate.||||||
15129|Petrie Formation|44912|14|Not recorded|E12-B-7,8|||||||||
15129|Petrie Formation|45087|5|Briefly described|p172|||Chemical analyses||||||
15129|Petrie Formation|61155|5|Briefly described|p19|Middle Eocene|Early Eocene|Overlies part of the Silkstone Formation. Age: ~56-46Ma. Thickness: 300m. In the Brisbane region.||||||
15129|Petrie Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
15129|Petrie Formation|69599|5|Briefly described|p586, p594, p645|Eocene|Paleocene|Jones (1926) and others. Petrie Basin; N margins of Brisbane. Has a composite type section based on drill holes NS19 and Standard Gas Aspley Scout No.1; total thickness ~293m. Generally flat-lying; faults in the SW produce dips of almost 60 degrees. Diverse fossils listed. RELATED UNITS (continued): Also correlated (at least partly) with Flinders Dolomite; Oakdale Sandstone; Elliott and Lowmead Formations; Booval Group.|57 +/- 3 Ma (40Ar/39Ar: Cohen, 2007).|||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds; see COMMENTS for more.|Mudstone, siltstone and sandstone (~100m), overlain by extrusive basalt and interbedded limestone (~68m), then mudstone, oil shale, claystone, grit, minor limestone and brown coal (~115m), then ~10m of basalt.|
15141|Philpott Limestone|24076|5|Briefly described|p397 Fig. 2|Middle Devonian|Middle Devonian|Max. thickness: 610m.  Geological Province: Yarrol Basin.||||||
15141|Philpott Limestone|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
15141|Philpott Limestone|33774|3|Fully described|p11|||||||||
15141|Philpott Limestone|33905|6|Mentioned|p265|||||||||
15141|Philpott Limestone|35008|5|Briefly described|p175|||||||||
15141|Philpott Limestone|36333|6|Mentioned|Map legend|Middle Devonian|Early Devonian|||||||15-JUL-04
15141|Philpott Limestone|39445|5|Briefly described|Table 5|||||||||
15141|Philpott Limestone|42031|5|Briefly described|Fig.3 P759|||||||||
15141|Philpott Limestone|42868|5|Briefly described|p28|||||||||
15141|Philpott Limestone|43008|5|Briefly described|map legend|||||||||
15141|Philpott Limestone|44628|14|Not recorded|p109,Tb.||Emsian|||||||
15141|Philpott Limestone|61761|6|Mentioned|p4, p5|Early Devonian|Middle Devonian|Geological Province: Philpott Block, Gamilaroi terrane.||||||07-FEB-11
15141|Philpott Limestone|68679|5|Briefly described|p317|Middle Devonian|Middle Devonian|Driscoll (1960). Northern Philpott Subprovince.|||||Mainly basaltic and andesitic volcaniclastics with some possible lava and lesser lithic sandstone, mudstone and limestone.|
15146|Phonolite Hill phonolite|37386|6|Mentioned|Fig.2|||||||||
15146|Phonolite Hill phonolite|38310|6|Mentioned|p237|||||||||
15153|Piccadilly Formation|23422|5|Briefly described|p180, p205 Table 6.3|Early Carboniferous|Late Devonian|Of Keelbottom Group.||||||
15153|Piccadilly Formation|23424|6|Mentioned|p346|||||||||
15153|Piccadilly Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Keelbottom Group.||||||
15153|Piccadilly Formation|23893|5|Briefly described|p16|Early Carboniferous|Late Devonian|Of Keelbottom Group.  Geological Province: Burdekin Basin.||||||
15153|Piccadilly Formation|24074|5|Briefly described|p391 Table 2|Tournaisian|Famennian|Maximum thickness: 520m.  Geological Province: Burdekin Basin.||||||
15153|Piccadilly Formation|24577|4|Described|p755 Fig. 2, p760|Visean|Tournaisian|Of the Keelbottom Group. Overlain by the Percy Creek Formation. Overlies the Hardwick Formation. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
15153|Piccadilly Formation|24613|2|Defined|p9 Fig. 4, p67-68|Tournaisian|Tournaisian|Of Keelbottom Group. Conformably/gradationally overlies Hardwick Fm. Thickness: ~850m. Geological province: Burdekin Basin. Detailed lithology included for this sandstone, conglomerate, mudstone unit; contains plant fossils.||||||07-FEB-11
15153|Piccadilly Formation|24614|5|Briefly described|p191 Fig. 1|Tournaisian|Tournaisian|Of the Keelbottom Group. Geological Province: Burdekin Basin. See also p196 Fig. 5.||||||07-FEB-11
15153|Piccadilly Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
15153|Piccadilly Formation|31285|4|Described|p82|||Tournaisian||||||
15153|Piccadilly Formation|31999|6|Mentioned|p193|||Table 11||||||
15153|Piccadilly Formation|32140|5|Briefly described|p7|||Carb. Refers Wyall et al. (1965)||||||
15153|Piccadilly Formation|32169|6|Mentioned|Table 2|||L.Carb.||||||
15153|Piccadilly Formation|32553|4|Described|p46|||||||||
15153|Piccadilly Formation|35811|6|Mentioned|Fig.3|||||||||
15153|Piccadilly Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
15153|Piccadilly Formation|37573|3|Fully described|p218|||See also Fig.14||||||
15153|Piccadilly Formation|39445|5|Briefly described|Table 6|||||||||
15153|Piccadilly Formation|39686|6|Mentioned|p72|||||||||
15153|Piccadilly Formation|42547|4|Described|p66|||||||||
15153|Piccadilly Formation|42689|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
15153|Piccadilly Formation|42933|6|Mentioned|p172|||See also misspelling Picadilly Formation Fig.94 p258.||||||
15153|Piccadilly Formation|43095|5|Briefly described|Plate 1|||of Keelbottom Group||||||
15153|Piccadilly Formation|43933|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Of Keelbottom Group.||||||
15153|Piccadilly Formation|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
15153|Piccadilly Formation|44061|4|Described|Table 2||Early Carboniferous|||||||
15153|Piccadilly Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
15153|Piccadilly Formation|45151|5|Briefly described|Table 6|||||||||
15153|Piccadilly Formation|46845|6|Mentioned|Table 1|||||||||
15153|Piccadilly Formation|48904|6|Mentioned|p20|||||||||
15153|Piccadilly Formation|67402|4|Described|p239, p246, p247, p248|Tournaisian|Tournaisian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in breaided-river plain or delta conditions.||||Overlies the Hardwick Formation.|Sandstones, pebbly sandstones, conglomerate and rare siltstones and mudstones.|
15153|Piccadilly Formation|68419|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin.||Of the Keelbottom Group.||Conformably underlain by the Hardwick Formation.|Pebbly quartzose and feldspathic sandstone, polymictic conglomerate and mudstone; plant fossils.|
15153|Piccadilly Formation|68420|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Burdekin Basin. But map symbol implies entirely Early Carboniferous (Ckp)||Of the Keelbottom Group.||Conformably underlain by the Hardwick Formation.|Pebbly quartzose and feldspathic sandstone, polymictic conglomerate and mudstone; plant fossils.|27-AUG-14
15153|Piccadilly Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4|Mississippian|Mississippian|Burdekin Basin. < 850 m thick. Braidplain, locally deltaic. Pebbles and cobbles mainly basement lithologies with some volcanics. Paleocurrent determinations indicate transport towards the east.||Of the Keelbottom Group.|||Comprises medium-grained to very coarse grained quartzose to sublabile sandstone, commonly pebbly to cobbly. Uncommon fine sandstone interbeds.|
15163|Pickwick Metabasalt Member|23031|6|Mentioned|24|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt. Of the Eastern Creek Volcanics.||||||07-NOV-08
15163|Pickwick Metabasalt Member|23395|5|Briefly described|p386 Fig.3|||Of the Eastern Creek Volcanics.||||||23-NOV-06
15163|Pickwick Metabasalt Member|23518|4|Described|p11|Proterozoic|Proterozoic|Of Eastern Creek Volcanics.  Geological Province: Western Fold Belt.||||||
15163|Pickwick Metabasalt Member|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics.  Overlies the Lena Quartzite Member.||||||25-AUG-04
15163|Pickwick Metabasalt Member|30534|2|Defined|p303|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|33900|5|Briefly described|p11|||||||||
15163|Pickwick Metabasalt Member|35295|6|Mentioned|Fig.2|||||||||
15163|Pickwick Metabasalt Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|37568|5|Briefly described|p81|||||||||
15163|Pickwick Metabasalt Member|38232|6|Mentioned|p84|||||||||
15163|Pickwick Metabasalt Member|38233|5|Briefly described|Table 1|||||||||
15163|Pickwick Metabasalt Member|38234|6|Mentioned|p103|||||||||
15163|Pickwick Metabasalt Member|38236|6|Mentioned|p120|||||||||
15163|Pickwick Metabasalt Member|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Eastern Creek Volcanics. Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite.||||||23-NOV-06
15163|Pickwick Metabasalt Member|39622|6|Mentioned|p30|||See also Appendix||||||
15163|Pickwick Metabasalt Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
15163|Pickwick Metabasalt Member|39924|6|Mentioned|p348|||||||||
15163|Pickwick Metabasalt Member|39934|6|Mentioned|p317|||||||||
15163|Pickwick Metabasalt Member|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15163|Pickwick Metabasalt Member|40221|3|Fully described|p7|||||||||
15163|Pickwick Metabasalt Member|40598|6|Mentioned|Fig.2|||||||||
15163|Pickwick Metabasalt Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
15163|Pickwick Metabasalt Member|45136|4|Described|p47|||||||||
15163|Pickwick Metabasalt Member|45166|5|Briefly described|p15|||||||||
15163|Pickwick Metabasalt Member|46801|6|Mentioned|p123|||||||||
15163|Pickwick Metabasalt Member|47083|4|Described|p5 + p6|||Youngest member of Eastern Creek Volcanics. Of Eastern Creek Volcanics of the Haslingden Group. Conformably overlain by Alsace Quartzite. Maximum thickness: 250 m.||||||23-NOV-06
15163|Pickwick Metabasalt Member|49041|6|Mentioned|Table 4|||||||||
15163|Pickwick Metabasalt Member|50100|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Eastern Creek Volcanics.||||||
15163|Pickwick Metabasalt Member|62873|5|Briefly described|p692, p704|Paleoproterozoic|Paleoproterozoic|Of the Eastern Creek Volcanics.  Overlies the Lena Quartzite Member.||||||07-NOV-08
15163|Pickwick Metabasalt Member|63023|5|Briefly described|p1025 Fig. 2|||Of Eastern Creek Volcanics (Haslingden Group). Geological Province: Leichardt Superbasin.||||||
15163|Pickwick Metabasalt Member|63111|5|Briefly described|p1164 Tb. 1|Statherian|Statherian|Of Eastern Creek Volcanics. Overlain by Lena Quartzite Member. Geological Province: Leichhardt Superbasin. Tholeiitic mafic intrusions comprising metabasalts, sediments and tuffs.||||||07-FEB-11
15163|Pickwick Metabasalt Member|64367|5|Briefly described|p555  Fig. 1b|Paleoproterozoic|Paleoproterozoic|See also Pickwick Member. The abbreviated version of the name is used throughout the text - all relevant details are therefore attached to that version of the name. Also referred to as the Pickwick basalts. Of Eastern Creek Volcanics.||||||07-FEB-11
15163|Pickwick Metabasalt Member|64832|5|Briefly described|p1154, p1155 Figs. 2, 3|Paleoproterozoic|Paleoproterozoic|Of the Eastern Creek Volcanics. Geological Province: Mt Isa Inlier. Has lower titanium content than Cromwell Metabasalt Member, but extremely high Cu concentrations in its upper section - detailed geochemistry included. Referred to throughout paper.||||||07-FEB-11
15163|Pickwick Metabasalt Member|67323|5|Briefly described|GIS attrib tbl, p13|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Leichhardt Superbasin.||Eastern Creek Formation.||Overlies Lena Quartzite Member.|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia, tuff|
15163|Pickwick Metabasalt Member|67499|6|Mentioned|p938|||||Of the Eastern Creek Volcanics.||||08-MAY-12
15163|Pickwick Metabasalt Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
15163|Pickwick Metabasalt Member|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Lena Quartzite Member. Is overlain by Alsace Quartzite (Myally Subgroup).|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia and tuff. (Separately mapped) quartzite, feldspathic sandstone and epidosite.|
15163|Pickwick Metabasalt Member|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Eastern Creek Volcanics.||Overlies Lena Quartzite Member. Is overlain by Alsace Quartzite (Myally Subgroup).|Grey-green metabasalt, red-brown trachybasalt, orthoquartzite, feldspathic quartzite, amygdaloidal metabasalt, flow-top breccia and tuff. (Separately mapped) quartzite, feldspathic sandstone and epidosite.|
15163|Pickwick Metabasalt Member|71799|4|Described|p150 fig 2, p152, p156, p157-p158|Statherian|Statherian|Lawn Hill.|ca. 1775 Ma|Eastern Creek Volcanics||Overlies the Lena Quartzite Member. Overlain by the Alsace Quartzite.|Peperite, hyaloclastite and basalts.|03-OCT-18
15163|Pickwick Metabasalt Member|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|||Of Eastern Creek Volcanics|||metabasalt; fluviolacustrine sandstone between basalt flows.|
15163|Pickwick Metabasalt Member|73553|5|Briefly described|p231 Fig.7.1.7|||Western Succession.||Eastern Creek Volcanics||||
15176|Piebald Basalt|23423|5|Briefly described|p312 Table 7.4||Cenozoic|Also see p261. Piebald Subprovince.||||||19-NOV-08
15176|Piebald Basalt|23511|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
15176|Piebald Basalt|31832|6|Mentioned|Table 6|||||||||
15176|Piebald Basalt|34046|6|Mentioned|Table III|||||||||
15176|Piebald Basalt|37603|5|Briefly described|p438|||||||||
15176|Piebald Basalt|37607|6|Mentioned|Fig.6|||||||||
15176|Piebald Basalt|39445|5|Briefly described|Table 14|||||||||
15176|Piebald Basalt|42369|5|Briefly described|Table 5, P73, P57|||Also Fig.3, p18.||||||07-SEP-18
15176|Piebald Basalt|43070|5|Briefly described|p7|||||||||
15176|Piebald Basalt|43896|14|Not recorded|Map Legend|Quaternary|Tertiary|||||||
15176|Piebald Basalt|43979|4|Described|p65-67,69,70,75||Cenozoic|||||||19-NOV-08
15176|Piebald Basalt|44267|14|Not recorded|Map Legend||Cenozoic|Undifferentiated Cainozoic.||||||19-NOV-08
15176|Piebald Basalt|44292|2|Defined|Tb.1,p12,map||Cenozoic|Correlated with McLean and Atherton Basalts.||||||19-NOV-08
15176|Piebald Basalt|44293|14|Not recorded|Map Legend||Tertiary|||||||
15176|Piebald Basalt|44294|2|Defined|Tb.2,p16,map||Tertiary|||||||
15176|Piebald Basalt|44872|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
15176|Piebald Basalt|45025|6|Mentioned|p33|||Ref. to Jack 1884.||||||
15176|Piebald Basalt|45087|5|Briefly described|p180|||Chemical analyses||||||
15176|Piebald Basalt|50587|5|Briefly described|Map Legend|Pleistocene|Pliocene|Alkali basalt, transitional basalt, olivine tholeiite, hawaiite, mugearite; minor scoria, alluvium.||||||28-JUN-04
15176|Piebald Basalt|60425|4|Described|p42 Tb. 3, p55 Tb. 4|Middle Pleistocene|Late Pliocene|Unconformable on Hodgkinson Formation and Yates Supersuite rocks. Age: ~3-1.2Ma (K-Ar). Thickness: ~50m? Geological province: Laura Basin.  Alkali basalt, transitional basalt, olivine tholeiite, hawaiite, mugearite, scoria; minor alluvium (at base).||||||07-FEB-11
15176|Piebald Basalt|61155|5|Briefly described|p20|Pleistocene|Late Pliocene|In eastern Cape York.||||||
15176|Piebald Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, Chudleigh, McIvor River, McLean, Sturgeon and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
15176|Piebald Basalt|69599|5|Briefly described|p642|||W of Hopevale, Piebald Province.|1.6-1.2 Ma (Stephenson, 1989).||||Basanite, hawaiite, mugearite and minor olivine tholeiite. Dominated by numerous pyroclastic and composite vent-type eruptions.|
15176|Piebald Basalt|72298|6|Mentioned|p792|||The town water supply at Hopevale is sourced from this unit and the fine sand underlying it.||||||
15176|Piebald Basalt|72983|6|Mentioned|p35|Cainozoic|Cainozoic|||||Underlain by Hope Vale Granite.||
15185|Pikedale beds|42559|4|Described|p9|||Stated to be informal name. Permian?||||||
15185|Pikedale beds|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic (locally pebbly) arenite, conglomerate and mudstone; rare vitric tuff.||||||11-DEC-07
15185|Pikedale beds|63748|5|Briefly described|p16, p18|Early Permian|Early Permian|Unconformably overlie Texas beds basement. Comprise lithic arenite, siltstone and mudstone, interlayered with sporadic discontinuous pebbly, conglomeratic lenses. Also mentioned: p68.||||||07-FEB-11
15185|Pikedale beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Bondonga, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
15185|Pikedale beds|68679|5|Briefly described|p452, p455|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Forms a narrow, NNW-trending, partly fault-bounded wedge of sediments 30km W of Stanthorpe. Has open, gently plunging folds and moderate to locally steep dips. Fossil wood and other plant remains. Age from similarity with other Permian outliers.||||Unconformably overlies or is faulted against Texas beds.|Lithic sandstone, siltstone and mudstone, interlayered with sporadic discontinuous pebbly conglomerate lenses and local vitric tuff.|
15185|Pikedale beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||27-SEP-18
15185|Pikedale beds|70373|4|Described|p789-p792, p795, p797 Tb 1, p798-p804|Early Permian|Early Permian|No fossils reported, so early Permian age inferred from lithological similarities to other Permian units. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. 280-320m thick.|289.7 +/-9.9 Ma (LA-ICP-MS on zircons)|||Assumed to overlie Texas beds, contact probably faulted. Correlated with Bondonga, Silver Spur, Terrica and Alum Rock beds.|Sandstone, pebbly sandstone, conglomerate, diamictite and mudstone with clasts of chert, sandstone and volcanics.|
15212|Pilliga Sandstone|721|5|Briefly described|Map legend|Tithonian|Oxfordian|Geological Province: Surat Basin.||||||11-NOV-14
15212|Pilliga Sandstone|730|6|Mentioned|p24.|||Fluviatile.||||||11-NOV-14
15212|Pilliga Sandstone|12597|5|Briefly described|p492 Tb.1, p494, p497|Tithonian|Oxfordian|S Surat Basin. 100-300m thick.||||Interfingers with Kumbarilla beds.|Quartzose sandstone with minor interbeds of siltstone and mudstone; thin pebble conglomerate bands occur throughout.|
15212|Pilliga Sandstone|22831|4|Described|p 84|Jurassic|Jurassic|Overlain by Cainozoic sediments.||||||17-SEP-08
15212|Pilliga Sandstone|22857|4|Described|p295, p296-7 Tb 22.1, p546 Tb A1.12|Late Jurassic|Callovian|Of the Injune Creek Group. Fullers earth occurs in a thin horizon. Merges with Gubberamunda Sandstone from Qld. Max. thickness: 300m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5..||||||
15212|Pilliga Sandstone|22865|4|Described|p295,Table22.1p296-7|Tithonian|Callovian|||||||
15212|Pilliga Sandstone|23016|6|Mentioned|p316||Jurassic|||||||
15212|Pilliga Sandstone|23043|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|of Surat Basin.||||||
15212|Pilliga Sandstone|23050|4|Described|p23 Table 4|Late Jurassic|Late Jurassic|of Surat Basin. Palnology indicates a J5 Jurassic age.||||||
15212|Pilliga Sandstone|23051|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|of Surat Basin.||||||
15212|Pilliga Sandstone|23053|4|Described|p8,10,25-6,57|Late Jurassic|Middle Jurassic|||||||
15212|Pilliga Sandstone|23170|2|Defined|p332|Late Jurassic|Late Jurassic|Of Surat Basin. Age from microfloral assemblage.||||||23-SEP-18
15212|Pilliga Sandstone|23214|6|Mentioned|p271|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
15212|Pilliga Sandstone|23566|5|Briefly described|p116 Fig. 2|Jurassic|Jurassic|Geological Province: Gunnedah Basin||||||
15212|Pilliga Sandstone|23740|5|Briefly described|p1220|Jurassic|Jurassic|Geological Province: Gunnedah Basin||||||
15212|Pilliga Sandstone|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
15212|Pilliga Sandstone|23883|6|Mentioned|p134|||Geological Province: Great Australian Superbasin.||||||
15212|Pilliga Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
15212|Pilliga Sandstone|24042|5|Briefly described|p510|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
15212|Pilliga Sandstone|24092|5|Briefly described|p8 Fig.3|||||||||
15212|Pilliga Sandstone|24126|5|Briefly described|p5|Jurassic|Triassic|||||||
15212|Pilliga Sandstone|24159|5|Briefly described|p148 Fig.2|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin. Underlying Unit: Walloon Coal Measures.||||||
15212|Pilliga Sandstone|29591|6|Mentioned|p75|||||||||
15212|Pilliga Sandstone|29869|6|Mentioned|Fig.1|||||||||
15212|Pilliga Sandstone|29870|6|Mentioned|p15|||||||||
15212|Pilliga Sandstone|29909|6|Mentioned|p145|||||||||
15212|Pilliga Sandstone|29986|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|29993|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30135|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30608|5|Briefly described|p116|||Lithology||||||
15212|Pilliga Sandstone|30610|1|Redefined|p322|Late Jurassic|Late Jurassic|||||||
15212|Pilliga Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
15212|Pilliga Sandstone|30699|6|Mentioned|p56|||Map||||||
15212|Pilliga Sandstone|30910|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|31326|4|Described|p38|||Jurassic||||||
15212|Pilliga Sandstone|31376|6|Mentioned|p4|||||||||
15212|Pilliga Sandstone|31726|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32045|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32482|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32944|6|Mentioned|Fig.2|||||||||
15212|Pilliga Sandstone|33169|6|Mentioned|p322|||||||||
15212|Pilliga Sandstone|33676|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|33709|6|Mentioned|p102|||||||||
15212|Pilliga Sandstone|33873|6|Mentioned|p5|||||||||
15212|Pilliga Sandstone|34059|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic.||||||
15212|Pilliga Sandstone|34244|6|Mentioned|p299|||Jur. Aquifer. See also P300||||||
15212|Pilliga Sandstone|34254|6|Mentioned|p491|||||||||
15212|Pilliga Sandstone|34394|6|Mentioned|Fig.43|||Refers Dulhunty (1967).||||||
15212|Pilliga Sandstone|34444|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|34982|6|Mentioned|p49|||||||||
15212|Pilliga Sandstone|35065|6|Mentioned|p45|||||||||
15212|Pilliga Sandstone|35095|6|Mentioned|p108|||||||||
15212|Pilliga Sandstone|35587|6|Mentioned|p44|||||||||
15212|Pilliga Sandstone|36570|2|Defined|p39|Jurassic|Jurassic|See p25, Fig.9.||||||22-SEP-18
15212|Pilliga Sandstone|36751|6|Mentioned|p488|||||||||
15212|Pilliga Sandstone|36961|6|Mentioned|Table 1|||||||||
15212|Pilliga Sandstone|37437|5|Briefly described|p29|||||||||
15212|Pilliga Sandstone|37794|4|Described|p191|||||||||
15212|Pilliga Sandstone|37856|6|Mentioned|Table I|||||||||
15212|Pilliga Sandstone|37995|6|Mentioned|p62|||||||||
15212|Pilliga Sandstone|38689|6|Mentioned|p308|||||||||
15212|Pilliga Sandstone|38813|5|Briefly described|p251|||||||||
15212|Pilliga Sandstone|39063|6|Mentioned|Fig.6|||||||||
15212|Pilliga Sandstone|39212|6|Mentioned|p25|||Aquifer||||||
15212|Pilliga Sandstone|39315|6|Mentioned|Fig.5|||||||||
15212|Pilliga Sandstone|39445|5|Briefly described|Table 10|||||||||
15212|Pilliga Sandstone|39664|6|Mentioned|p120|||||||||
15212|Pilliga Sandstone|39666|6|Mentioned|p94|||See also P112||||||
15212|Pilliga Sandstone|39913|6|Mentioned|Fig.1|||||||||
15212|Pilliga Sandstone|40328|6|Mentioned|p213|||||||||
15212|Pilliga Sandstone|40365|6|Mentioned|p245|||See also P293||||||
15212|Pilliga Sandstone|40767|6|Mentioned|p2|||||||||
15212|Pilliga Sandstone|40869|6|Mentioned|p29|||||||||
15212|Pilliga Sandstone|40952|6|Mentioned|p3|||||||||
15212|Pilliga Sandstone|40953|6|Mentioned|p19|||||||||
15212|Pilliga Sandstone|41266|6|Mentioned|Fig.3|||||||||
15212|Pilliga Sandstone|41290|5|Briefly described|p227|||||||||
15212|Pilliga Sandstone|41330|6|Mentioned|p21|||||||||
15212|Pilliga Sandstone|41779|6|Mentioned|p183|||||||||
15212|Pilliga Sandstone|42135|6|Mentioned|Fig.6 P357|||||||||
15212|Pilliga Sandstone|42596|5|Briefly described|Fig. 1 P24|||||||||
15212|Pilliga Sandstone|42657|6|Mentioned|p73|||||||||
15212|Pilliga Sandstone|42679|6|Mentioned|Fig.4 P3|||||||||
15212|Pilliga Sandstone|42918|6|Mentioned|p45|||||||||
15212|Pilliga Sandstone|43044|6|Mentioned|p121|||||||||
15212|Pilliga Sandstone|43091|5|Briefly described|Map Legend|||of Surat Basin||||||
15212|Pilliga Sandstone|43161|6|Mentioned|21-26||Jurassic|||||||
15212|Pilliga Sandstone|43194|5|Briefly described|p122|Jurassic|Jurassic|Gunnedah Basin. Disconformably overlies Napperby Formation.||||||
15212|Pilliga Sandstone|43276|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|||||||
15212|Pilliga Sandstone|43277|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|of Great Australian Basin.||||||
15212|Pilliga Sandstone|43354|5|Briefly described|p105-108,p107||Jurassic|||||||
15212|Pilliga Sandstone|43355|14|Not recorded|Map Legend||Jurassic|Provisional Edition||||||
15212|Pilliga Sandstone|43356|14|Not recorded|Map Legend||Jurassic|||||||
15212|Pilliga Sandstone|43383|14|Not recorded|p25||Jurassic|||||||
15212|Pilliga Sandstone|43393|14|Not recorded|p179-182||Jurassic|||||||
15212|Pilliga Sandstone|43394|14|Not recorded|p105-108||Jurassic|||||||
15212|Pilliga Sandstone|43404|14|Not recorded|Table p11|Cretaceous|Jurassic|||||||
15212|Pilliga Sandstone|43405|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43407|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43410|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43476|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43494|4|Described|p14|Late Jurassic|Late Jurassic|Lower lithic sandstone and polymictic conglomerate; and upper more quartz-rich rock, particularly the basal bed which is a very coarse quartz sandstone containing rounded qtz pebbles and subangular qtz granules. Overlies Pulrawaugh Fm. Max. thick: 100m.||||||16-MAR-06
15212|Pilliga Sandstone|43500|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43534|14|Not recorded|p393,394|||||||||
15212|Pilliga Sandstone|43535|14|Not recorded|p133-136||Jurassic|||||||
15212|Pilliga Sandstone|43582|6|Mentioned|Fig.5,p16||Late Jurassic|||||||
15212|Pilliga Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
15212|Pilliga Sandstone|43678|6|Mentioned|p316||Jurassic|||||||
15212|Pilliga Sandstone|44028|14|Not recorded|p514|||Equivalent of Gubberamunda Sandstone. See Strat Table.||||||
15212|Pilliga Sandstone|44160|6|Mentioned|Map Legend||Jurassic|||||||
15212|Pilliga Sandstone|44450|6|Mentioned|p27|||Geological Province: Great Australian Basin.||||||
15212|Pilliga Sandstone|45110|2|Defined|p98|Late Jurassic|Late Jurassic|Formerly Pilliga Series (Kenny,1928), Pilliga Beds (Dulhunty,1939).||||||11-NOV-14
15212|Pilliga Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
15212|Pilliga Sandstone|48958|6|Mentioned|Plate 1|||||||||
15212|Pilliga Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
15212|Pilliga Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
15212|Pilliga Sandstone|49781|6|Mentioned|p4|||||||||
15212|Pilliga Sandstone|50590|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Great Australian Basin (possibly misspelt) .  Massive to cross-bedded coarse pebbly lithic-quartz sandstone, minor lithic sandstone and siltstone.||||||
15212|Pilliga Sandstone|50616|5|Briefly described|p275, 286|Jurassic|Jurassic|Interbedded sandstone and thicker shale and mudstone units.||||||
15212|Pilliga Sandstone|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin. Overlies: Purlawaugh Formation.||||||05-JUL-04
15212|Pilliga Sandstone|60266|5|Briefly described|p2,  p3 Tb. 1|Late Jurassic|Middle Jurassic|Piedmont deposits of quartzose sandstone and conglomerate.  Overlies Purlawaugh Formation; underlies the Keelindi beds.  Geological Province: Surat Basin.||||||08-DEC-04
15212|Pilliga Sandstone|60267|4|Described|p15|Jurassic|Jurassic|Quartz-rich sandstone conglomerate with siliceous clasts of vein quartz, chert and jasper.  Overlies Garrawilla Volcs; conformably overlain by Keelindi beds; also overlain by Warrumbungle Volcs.  Max. thickness:>100m.  Geol.Prov: Surat Basin.||||||
15212|Pilliga Sandstone|61313|5|Briefly described|p91, p94 Fig.G7|Late Jurassic|Middle Jurassic|Stacked sequence of braided fluvial sandstones with reservoir qualities but lacks laterally continuous seals. Conformably overlies Purlawaugh Sandstone; conformably overlain by Orallo and Mooga Fms. Thickness: 213m. Geol. Prov: Gunnedah and Surat Basins.||||||
15212|Pilliga Sandstone|61377|5|Briefly described|p152, p154 Fig. SU9|Late Jurassic|Middle Jurassic|Massive quartzose sandstones; minor siltstone and mudstone. Conformably overlies the Walloon Coal Measures; conformably overlain by Orallo, Mooga, Bungil and Wallumbilla Formations. Geological Province: Surat Basin. See also p148 Tb. SU1, p149 Fig. SU8.||||||07-FEB-11
15212|Pilliga Sandstone|61776|5|Briefly described|p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Quartz-sandstone with minor lithic sandstone and siltstone.||||||17-SEP-08
15212|Pilliga Sandstone|62534|5|Briefly described|p10 (legend)|Late Jurassic|Late Jurassic|Geological Province: Surat Basin. Quartzose sandstone.||||||07-FEB-11
15212|Pilliga Sandstone|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
15212|Pilliga Sandstone|63733|5|Briefly described|Map legend|Jurassic|Jurassic|Quartzose sandstone, conglomerate.||||||
15212|Pilliga Sandstone|64856|6|Mentioned|p90, p93|||Interfingers with Springbok Sandstone.|| ||||29-NOV-17
15212|Pilliga Sandstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Late Jurassic|Unit in the Surat Basin. Underlies the Orallo Formation in NSW; overlies the Purlawaugh Formation.||||||22-MAR-12
15212|Pilliga Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Late Jurassic|Overlies the Purlawaugh Formation, underlies the Orallo Formation.||||||
15212|Pilliga Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous|Late Jurassic|||||||
15212|Pilliga Sandstone|65116|4|Described|p456, Fig 2 p437|Early Cretaceous|Late Jurassic|Underlies the Orallo Formation, overlies the Purlawaugh Formation, Surat Basin. Equivalent to Springbok Sst + Westbourne Formation + Gubberamunda Formation. Medium to coarse-grained quartzose sandstone.||||||
15212|Pilliga Sandstone|65119|6|Mentioned|p504 Table 1|Late Jurassic|Early Jurassic|Age: 177-150 Ma. Fission Track age: 187+/-13 Ma.||||||20-MAR-13
15212|Pilliga Sandstone|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment and Surat Basin.||||Overlies Walloon Coal Measures and Purlawaugh Formation. Is overlain by Kumbarilla beds and Keelindi Beds.||
15212|Pilliga Sandstone|68003|5|Briefly described|p52, pp54-57 Figs, pp64-66, p98, p127.|Late Jurassic|Middle Jurassic|Crops out over much of the Brigalow Belt South Bioregion. Forms cliffs.||||Conformably overlies Walloon Coal Measures and Purlawaugh Formation. Is conformably overlain by Keelindi beds and Orallo Formation.|Coarse-grained, quartzose, braided-stream sandstone; basal pebble lenses common; minor interbeds of siltstone and mudstone; common carbonaceous fragments and iron staining.|
15212|Pilliga Sandstone|68004|5|Briefly described|p87, p174, p182.|Late Jurassic|Late Jurassic|Excellent reservoir potential; sealed by the Orallo Formation but this becomes more sandy towards its depositional limits. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows.|||||Widespread, excellent quality quartz sandstone.|
15212|Pilliga Sandstone|68005|5|Briefly described|p131.|Jurassic|Jurassic|Surat Basin.|||||Medium to coarse, cross-bedded quartzose sandstone with basal pebble lenses common; minor interbeds of siltstone and mudstone.|
15212|Pilliga Sandstone|68006|5|Briefly described|p92.|||Bores targetting this unit for water have intersected coal in the underlying Walloon Coal Measures.||||Overlies Walloon Coal Measures.||
15212|Pilliga Sandstone|68069|5|Briefly described|Map legend.|Late Jurassic|Late Jurassic|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Braided to meandering river system with extensive flood plains.||||Conformably overlies Purlawaugh Formation. Is overlain conformably by Orallo Formation.|Medium- to coarse-grained, well-sorted quartzose sandstone with minor interbeds of mudstone, siltstone and fine-grained sandstone.|
15212|Pilliga Sandstone|68135|5|Briefly described|p52 fig 2b|Tithonian|Oxfordian|Surat Basin (NSW)||||Disconformably overlies Purlawaugh Formation, overlain by Orallo Formation|Cross-bedded sandstone.|14-SEP-17
15212|Pilliga Sandstone|68593|5|Briefly described|p3-4, p45, p47|Late Jurassic|Late Jurassic|Deposited by a braided to meandering river system with extensive flood plains. One of the main artesian aquifers in the map area.||||Overlies Purlawaugh Formation. Is overlain by Orallo Formation.|Medium- to coarse-grained, well-sorted quartzose sandstone with minor interbeds of mudstone, siltstone and fine-grained sandstone.|
15212|Pilliga Sandstone|68679|6|Mentioned|p455|Early Cretaceous|Early Jurassic|||||||
15212|Pilliga Sandstone|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
15212|Pilliga Sandstone|69594|5|Briefly described|p537|||Exon (1976).||||Interdigitates with and passes into Westbourne Formation.||
15212|Pilliga Sandstone|69790|6|Mentioned|p1070|Late Jurassic|Late Jurassic|||||Equivalent to Springbok Sandstone in Qld.||
15212|Pilliga Sandstone|70036|5|Briefly described|Map legend|Late Jurassic|Late Jurassic|Surat Basin. Included in a mapped unit of a braided stream sequence: quartzose sandstone with minor mudstone, siltstone and coal.||||||
15212|Pilliga Sandstone|70821|5|Briefly described|p22 Fig.2.7, p80|Jurassic|Jurassic|Surat Basin; Coonamble Embayment. Aquifer: generally artesian.||Injune Creek Group.||Overlies Walloon Coal Measures or Purlawaugh Formation. Is overlain by Westbourne or Orallo Formations, Kumbarilla or Keelindi beds.||
15212|Pilliga Sandstone|71628|5|Briefly described|p4: 33, 35|||Surat Basin.||||Overlies Graman and Linton Monzogranites.||
15212|Pilliga Sandstone|71890|4|Described|vi-vii, p5-p8, p18, p24, p26, p30|Kimmeridgian|Toarcian|Surat Basin. Interpreted to have been deposited in a braided stream system. Eroded prior to Miocene volcanism in the area. This unit is the most extensively exposed sedimentary unit in the present study's map area. This unit is typically an aquifer. See also  p33-p34, p39, p52.|177-150 Ma|||Disconformably overlies the Purlawaugh Formation. Conformably overlain by Keelindi beds. Overlies the Garrawilla Volcanics.|Medium- to very coarse grained, well sorted, quartzose sandstone and minor pebble conglomerate. Rare to minor thin interbeds of mudstone, siltstone and fine-grained sandstone.|13-JUN-22
15212|Pilliga Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||||Overlies Walloon Coal Measures and Purlawaugh FZ. Is overlain by Orallo FZ, Kumbarilla and Keelindi beds.||
15212|Pilliga Sandstone|72700|5|Briefly described|Mapsheet 1 and 2|Mesozoic|Palaeozoic||||||Commonly cross-bedded, medium to coarse-grained quartz sandstone and lesser conglomerate, minor mudstone, siltstone and coal.|
15212|Pilliga Sandstone|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in New South Wales.||||Overlies and partly laterally equivalent to Purlawaugh Formation and underlies Orallo Formation.|Includes fossiliferous sandstone.|
15212|Pilliga Sandstone|73492|6|Mentioned|p691|||||||||
15212|Pilliga Sandstone|73581|6|Mentioned|p12|||||||||
15225|Pilpah Sandstone|30479|6|Mentioned|Fig.3|||Refers Opik (1960).||||||
15225|Pilpah Sandstone|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15225|Pilpah Sandstone|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15225|Pilpah Sandstone|32659|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
15225|Pilpah Sandstone|32660|5|Briefly described|Table 5|||||||||
15225|Pilpah Sandstone|32959|6|Mentioned|Fig.21|||||||||
15225|Pilpah Sandstone|33214|6|Mentioned|Fig.1|||||||||
15225|Pilpah Sandstone|33900|6|Mentioned|p19|||||||||
15225|Pilpah Sandstone|34287|6|Mentioned|p41|||||||||
15225|Pilpah Sandstone|34395|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15225|Pilpah Sandstone|34754|6|Mentioned|p42|||||||||
15225|Pilpah Sandstone|35074|6|Mentioned|Fig.2|||||||||
15225|Pilpah Sandstone|35121|6|Mentioned|Map legend|Adelaidean|Adelaidean|Prob. Adelaidean||||||
15225|Pilpah Sandstone|35139|4|Described|Table.2|||||||||
15225|Pilpah Sandstone|35553|6|Mentioned|p177|||Appendix containing description of Agnostid localities.||||||
15225|Pilpah Sandstone|35950|6|Mentioned|p305|||||||||
15225|Pilpah Sandstone|37459|6|Mentioned|p427|||||||||
15225|Pilpah Sandstone|37462|4|Described|Table4.VII|||||||||
15225|Pilpah Sandstone|37565|5|Briefly described|p2|||||||||
15225|Pilpah Sandstone|37568|6|Mentioned|Fig.5|||||||||
15225|Pilpah Sandstone|37572|6|Mentioned|p165|||See also Fig.7||||||
15225|Pilpah Sandstone|39445|6|Mentioned|p55|||See also Table 3.||||||
15225|Pilpah Sandstone|44210|2|Defined|map,p5,6,9-16,Tb.1|||Possibly equivalent to Constance Sandstone.||||||
15225|Pilpah Sandstone|44211|14|Not recorded|p91,95-7|||See also Lexicon.||||||
15225|Pilpah Sandstone|44213|14|Not recorded|Map Legend||Neoproterozoic|||||||
15225|Pilpah Sandstone|44271|2|Defined|p36,40,52-3,55,62||Paleoproterozoic|See also Lexicon. Overlies Mingera Beds.||||||07-NOV-08
15225|Pilpah Sandstone|44275|14|Not recorded|Map Legend|||||||||
15225|Pilpah Sandstone|44285|14|Not recorded|p.6||Neoproterozoic|Mt. Isa sheet (F54-1). Upper Proterozoic.||||||
15225|Pilpah Sandstone|44290|14|Not recorded|p438,439|||||||||
15225|Pilpah Sandstone|44441|14|Not recorded|p.7||Neoproterozoic|Equivalent of either Pilpah Sandstone or Mittiebah Sandstone in BMR Well 11. Nearest exposure of Pilpah Sandstone is at F54-1 (Mt.Isa). Upper Proterozoic.||||||
15225|Pilpah Sandstone|44765|14|Not recorded|p16,18||Neoproterozoic|||||||
15225|Pilpah Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Adelaidean|||||||
15225|Pilpah Sandstone|44989|2|Defined|p.121|||Tb.II,III. On many pages. Redescribed. Overlies Paradise Creek Formation.;Underlies Camooweal Dolomite. (F54-1,E54-13).||||||
15225|Pilpah Sandstone|45052|4|Described|p73|||Adelaidean ?||||||
15225|Pilpah Sandstone|45055|6|Mentioned|p9|||Precambrian||||||
15225|Pilpah Sandstone|45166|5|Briefly described|p76|||||||||
15225|Pilpah Sandstone|45287|14|Not recorded|p.223,226,229|||||||||
15225|Pilpah Sandstone|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
15225|Pilpah Sandstone|49041|5|Briefly described|Table 1|||||||||
15227|Pinang Rhyolite|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
15227|Pinang Rhyolite|23161|4|Described|p21 table3|||||||||
15227|Pinang Rhyolite|42701|3|Fully described|p39|||Reserved as Pinang Rhyolite Member.||||||
15227|Pinang Rhyolite|44245|5|Briefly described|Map Legend||Carboniferous|||||||
15227|Pinang Rhyolite|60659|5|Briefly described|p16|||Of the Bulgonunna Volcanic Group. Moderately crystal-rich rhyolitic ignimbrite. Part of the Locharwood association. Of the Bulgonunna Province.||||||07-FEB-11
15227|Pinang Rhyolite|69593|5|Briefly described|p495|Permian|Late Carboniferous|The LITHOLOGY description is for the whole Group.|~305-293 Ma (SHRIMP U-Pb zircon).|Bulgonunna Volcanic Group.|||Voluminous lithics-rich to lithics-poor, variably crystal-rich, biotite-bearing rhyolitic and hornblende and/or biotite-bearing dacitic ignimbrites, lavas and domes; minor tuff, andesite, volcaniclastic sediments.|
15227|Pinang Rhyolite|70740|5|Briefly described|p88, p102|||Distribution is discussed briefly on p88. Thickness ranges from 20-40m.||Bulgonunna Volcanic Group||Overlies the Locharwood Rhyolite.|Light grey to brown and buff, moderately crystal-rich rhyolitic ignimbrite lacking eutaxitic texture.|
15253|Pinecliff Formation|23799|3|Fully described|p30|Early Permian|Early Permian|Of Cressbrook Creek Group. Contains the Kipper Creek Andesite Member.  Overlain by Hampton Road Rhyolite.  Intruded by Eskdale Granodiorite in west.  Max. thickness: ~1500m.||||||
15253|Pinecliff Formation|32912|6|Mentioned|p157|||L.Perm.||||||
15253|Pinecliff Formation|33381|4|Described|p108|||Perm. See also P111. Cressbrook Creek Gp.||||||
15253|Pinecliff Formation|39252|6|Mentioned|Fig.13|||||||||
15253|Pinecliff Formation|39445|5|Briefly described|Table 8|||||||||
15253|Pinecliff Formation|44555|2|Defined|p224|||See also Lexicon. Contains member Kipper Creek Andesite.||||||
15253|Pinecliff Formation|68679|5|Briefly described|p386|Guadalupian|Guadalupian|Cranfield et al. (2001). Cressbrook Basin. Marine, unstable shelf deposits: marine provenance. ~1500m thick.||Cressbrook Creek Group.||Is overlain unconformably by Hampton Road Rhyolite.|Chert, quartzite, and minor conglomerate and shale overlain by ~150m of basaltic pillow lavas and clastic deposits with rhyolitic clasts in upper parts; chert, conglomerate and minor coarse-grained feldspathic sandstone in upper part.|
15261|Pink Lily Sands|41576|5|Briefly described|p36|||||||||
15261|Pink Lily Sands|42054|6|Mentioned|p272|||||||||
15267|Pinnacles Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 311 +/- 5Ma, Rb-Sr.||||||
15267|Pinnacles Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 295. I-Type.||||||
15267|Pinnacles Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Brien's Creek Supersuite||||||
15267|Pinnacles Granite|40743|6|Mentioned|p318|||||||||
15267|Pinnacles Granite|41297|6|Mentioned|Fig.1|||||||||
15267|Pinnacles Granite|41824|6|Mentioned|p201|||||||||
15267|Pinnacles Granite|42532|4|Described|p304|||||||||
15267|Pinnacles Granite|43259|4|Described|Appendix 1,p36.||Carboniferous|||||||
15267|Pinnacles Granite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite).Age: 311+/-5Ma (Rb-Sr). I-type.Includes Askins Microgranite on most recent maps. Pink to yellow, medium-grained, porphyritic biotite granite.||||||07-FEB-11
15274|Pint Pot Andesite Member|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Thickness: Up to 150m. Geological Province: Georgetown Region.||||||28-MAY-15
15274|Pint Pot Andesite Member|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
15274|Pint Pot Andesite Member|43259|6|Mentioned|Appendix 1,p3.||Carboniferous|||||||
15274|Pint Pot Andesite Member|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Yellow Jacket Rhyolite (Eveleigh Volcanic Subgroup, Newcastle Range Volcanic Group).||||||
15274|Pint Pot Andesite Member|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Yellow Jacket Rhyolite.|||Greyish-green sparsely porphyritic hornblende-pyroxene andesite to basaltic andesite; probably includes intrusive equivalents.|
15286|Pipeclay Creek complex|40479|6|Mentioned|p33|||||||||
15286|Pipeclay Creek complex|40480|6|Mentioned|p41|||||||||
15286|Pipeclay Creek complex|40954|6|Mentioned|p133|||||||||
15306|Plain Creek Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: >1590Ma.||||||
15306|Plain Creek Formation|38237|6|Mentioned|Fig.3|||||||||
15306|Plain Creek Formation|38348|6|Mentioned|p18|||||||||
15306|Plain Creek Formation|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of McNamara Gp.  Fissile to flaggy, micaceous sltst. and shale with thin interbeds of ripple laminate sst; thicker interbeds of flaggy to blocky, well-sorted sst. with thin grit and pebbly bands. Overlies massive orthoquarzite within the McNamara Group.||||||10-JAN-05
15306|Plain Creek Formation|39497|4|Described|p11|||||||||
15306|Plain Creek Formation|39925|6|Mentioned|p334|||||||||
15306|Plain Creek Formation|45166|5|Briefly described|p76|||||||||
15306|Plain Creek Formation|49018|2|Defined|p8|Carpentarian|Carpentarian|||||||
15306|Plain Creek Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Micaceous siltstone and shale, fine to coarse grained lithic and sublithic sandstone; minor pebble conglomerate, graded sandstone beds, pebble to boulder bearing mudstone.||||||
15306|Plain Creek Formation|65337|3|Fully described|p9 Fig.5, pp27-28, p96.|Paleoproterozoic|Paleoproterozoic|Redefined; mapped in First Edition as part of Bluff Range beds. 400 - 1000 m of shallow to deep marine basin sediments including fan deltas. Manganese and iron oxide films and veins are common.|1647 +/- 8 to 1630 +/- 5 Ma.|Unit in McNamara Group.||Overlies Bullrush Conglomerate and Shady Bore Quartzite. Is overlain by Lawn Hill Formation and, unconformably, by Constance Sandstone.|Micaceous siltstone and shale, fine- to coarse-grained lithic and sublithic sandstone; minor pebble conglomerate, graded sandstone beds, and pebble- to boulder-bearing mudstone-turbidite and mass flow sediments.|
15306|Plain Creek Formation|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Isa Superbasin.||McNamara Group|||Siltstone, shale, sandstone.|
15306|Plain Creek Formation|69433|4|Described|p18:2, 5-6, 9-10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 400-1000m thick. A variety of facies is represented. Surficial manganese is common as a weathering crust; unlikely to extend deep into the host rock.||McNamara Group.||Conformably overlies Shady Bore Quartzite and (probably) Bullrush Conglomerate. Is overlain conformably by Lawn Hill Formation. Correlative of Buddycurrawa Volcanics (?).|Dominantly micaceous siltstone and shale, with several sandstone units. These sediments are arranged in cycles, a few metres thick, of stacked, upward-thickening and -coarsening beds. Thin films of manganese and iron oxides common throughout.|12-JUL-16
15306|Plain Creek Formation|69591|5|Briefly described|p54|||Camooweal-Murphy Domain, Isa Superbasin. Marine deposits.||McNamara Group.|||Siltstone, shale, sandstone.|
15306|Plain Creek Formation|69673|5|Briefly described|p52 fig 42, p53, p54, p55|||1km thick. Unconventional petroleum potential.||McNamara Group||Correlated with Riversleigh Siltstone, Termite Range Formation|Micaceous siltstone and shale, contains several sandstone units.|
15306|Plain Creek Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|||Siltstone, shale, sandstone|
15306|Plain Creek Formation|72526|5|Briefly described|p8 Fig.1.3, p10.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin.||McNamara Group||Overlies Shady Bore Quartzite and underlies Lawn Hill Formation.||
15306|Plain Creek Formation|72527|4|Described|p1, 8, 112, 119, p132-139, p193, 194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Characterised by 'interbeds' of shale, siltstone and sandstone  ranging in thickness from 400m to 1000m.|1635+/-13 max dep age c. 1647-1630|McNamara Group||Overlies Shady Bore Quartzite, Bullrush Conglomerate.  Underlies Lawn Hill Formation (presumed conformably) or Constance Sandstone (unconformably). Equivalent to Riversleigh Formation (or Siltstone).|Commonly cycles of feldspathetic and fine-grained flaggy sandstones and laminated siltstones. Also includes micaceous siltstone.|
15306|Plain Creek Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Shown as being located in the Northern Territory part of the McNamara Group.||McNamara Group||Overlies Shady Bore Quartzite and underlies Lawn Hill Formation. Laterally equivalent to Mount Les Siltstone, Riversliegh Siltstone.||
15306|Plain Creek Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Shady Bore Quartzite. Overlain by Lawn Hill Formation. Equivalent to Bullrush Conglomerate.||
15306|Plain Creek Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Partly underlain by Bullrush Conglomerate and Shady Bore Quartzite. Overlain by Lawn Hill Formation.||
15400|Police Creek Siltstone Member|30534|2|Defined|p305|Carpentarian|Carpentarian|||||||
15400|Police Creek Siltstone Member|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15400|Police Creek Siltstone Member|39622|6|Mentioned|Fig.2|||||||||
15400|Police Creek Siltstone Member|42676|5|Briefly described|Fig.2, P41|||||||||
15400|Police Creek Siltstone Member|45166|5|Briefly described|p16|||||||||
15400|Police Creek Siltstone Member|67323|5|Briefly described|GIS attrib tbl.|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.||Myally Subgroup.|||Siltstone, phyllite, rhyolitic tuff|
15406|Polland Waterhole Shale|23031|5|Briefly described|31|||Geol province Carpentaria Basin||||||
15406|Polland Waterhole Shale|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15406|Polland Waterhole Shale|34395|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15406|Polland Waterhole Shale|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15406|Polland Waterhole Shale|35139|4|Described|Table.2|||||||||
15406|Polland Waterhole Shale|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15406|Polland Waterhole Shale|37608|3|Fully described|Table 2|||||||||
15406|Polland Waterhole Shale|39445|5|Briefly described|Table 11|||||||||
15406|Polland Waterhole Shale|41298|6|Mentioned|Map legend|Cretaceous||||||||
15406|Polland Waterhole Shale|44210|2|Defined|map,5,7,12,13,Tb.2||Early Cretaceous|||||||
15406|Polland Waterhole Shale|44213|14|Not recorded|Map Legend||Early Cretaceous|||||||
15406|Polland Waterhole Shale|44275|14|Not recorded|Map Legend|||||||||
15406|Polland Waterhole Shale|44800|14|Not recorded|p32||Cretaceous|Equivalent.||||||
15406|Polland Waterhole Shale|44920|14|Not recorded|Map Legend, Sheet 2||Early Cretaceous|||||||
15406|Polland Waterhole Shale|45052|5|Briefly described|p134|||Mesozoic||||||
15406|Polland Waterhole Shale|45145|3|Fully described|Table 5|||||||||
15406|Polland Waterhole Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Cretaceous|Cretaceous|Eromanga/Carpentaria Basins|||||Claystone, siliceous shale, bioturbated glauconitic claystone|
15406|Polland Waterhole Shale|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Carpentaria Basin.||||Is overlain conformably by Normanton Formation.||
15406|Polland Waterhole Shale|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
15406|Polland Waterhole Shale|69594|6|Mentioned|p522|||Occurs on the CAMOOWEAL and MOUNT ISA 250k sheets. Known from the NT. Overlies Precambrian and Cambrian basement. Marine. May be up to 30m thick.||||||
15406|Polland Waterhole Shale|72912|6|Mentioned|p22|Cretaceous|Cretaceous|Overlies Georgina Basin rocks to southeast (CMP10780).||||||
15420|Pomegranate Limestone|22954|6|Mentioned|Fig3p9|Idamean|Idamean|||||||
15420|Pomegranate Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 396m.||||||
15420|Pomegranate Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
15420|Pomegranate Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15420|Pomegranate Limestone|31396|6|Mentioned|Fig.3|||||||||
15420|Pomegranate Limestone|31572|4|Described|Fig. 1|||U.Cambrian||||||
15420|Pomegranate Limestone|32952|6|Mentioned|p1188|||See also p1189. M.-U. Camb.||||||02-APR-07
15420|Pomegranate Limestone|33111|4|Described|p41|||||||||
15420|Pomegranate Limestone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
15420|Pomegranate Limestone|34847|6|Mentioned|Fig.6|||||||||
15420|Pomegranate Limestone|34903|6|Mentioned|p582|||||||||
15420|Pomegranate Limestone|35121|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
15420|Pomegranate Limestone|35139|4|Described|Table.2|||||||||
15420|Pomegranate Limestone|37155|6|Mentioned|p265|||||||||
15420|Pomegranate Limestone|37572|4|Described|p160|||See also Fig.8 and p165.||||||02-APR-07
15420|Pomegranate Limestone|38444|6|Mentioned|p139|||||||||
15420|Pomegranate Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15420|Pomegranate Limestone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|Overlain by Chatsworth Limestone; overlies O'Hara Shale unconformably.||||||25-AUG-04
15420|Pomegranate Limestone|39445|5|Briefly described|Table 4|||See also p64.||||||02-APR-07
15420|Pomegranate Limestone|39690|6|Mentioned|Fig.2|||||||||
15420|Pomegranate Limestone|40852|6|Mentioned|Fig.3.7|||||||||
15420|Pomegranate Limestone|41306|6|Mentioned|p4|||||||||
15420|Pomegranate Limestone|42139|6|Mentioned|Fig.9 P72|||||||||
15420|Pomegranate Limestone|43807|5|Briefly described|p345-6|||||||||
15420|Pomegranate Limestone|43883|14|Not recorded|p18 Fig.4-3|||Misspelt 'Pomegranite Ls' on bibliographic card.||||||
15420|Pomegranate Limestone|43995|14|Not recorded|p92,74||Late Carboniferous|||||||
15420|Pomegranate Limestone|44091|14|Not recorded|p17,Tb.1|Idamean|Mindyallan|||||||
15420|Pomegranate Limestone|44205|14|Not recorded|p14|||||||||02-APR-07
15420|Pomegranate Limestone|44211|2|Defined|p96,102,104|||||||||
15420|Pomegranate Limestone|44275|14|Not recorded|Map Legend|||||||||
15420|Pomegranate Limestone|44276|2|Defined|p18,22,Tb.2,map|||||||||
15420|Pomegranate Limestone|44277|14|Not recorded|Map Legend||Late Cambrian|||||||
15420|Pomegranate Limestone|44291|14|Not recorded|p7|||||||||
15420|Pomegranate Limestone|44361|14|Not recorded|Map Legend||Late Cambrian|||||||
15420|Pomegranate Limestone|44362|4|Described|p9,Tb.1||Late Cambrian|||||||
15420|Pomegranate Limestone|44920|14|Not recorded|Map Legend, Sheet 2||Late Cambrian|||||||
15420|Pomegranate Limestone|45002|14|Not recorded|p9-124|||See also Lexicon. Bituminous; early Late Cambrian fossils.||||||
15420|Pomegranate Limestone|45012|14|Not recorded|p99-102,120,152,154,|||p181,202,241,Fauna.||||||
15420|Pomegranate Limestone|45051|6|Mentioned|p4|||See also p6. Cambrian age||||||02-APR-07
15420|Pomegranate Limestone|45052|3|Fully described|p112|||U.Camb. See also p33.||||||02-APR-07
15420|Pomegranate Limestone|45053|6|Mentioned|p12|||||||||
15420|Pomegranate Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
15420|Pomegranate Limestone|45094|6|Mentioned|p11|||||||||
15420|Pomegranate Limestone|45130|6|Mentioned|p3|||||||||
15420|Pomegranate Limestone|45166|5|Briefly described|Table 15|||||||||
15420|Pomegranate Limestone|46958|6|Mentioned|Fig.2|||||||||
15420|Pomegranate Limestone|48906|14|Not recorded|Tb.1|||||||||
15420|Pomegranate Limestone|50100|5|Briefly described|p22|Early Ordovician|Late Cambrian|Sandy bituminous limestone sequence including micritic limestone, chert, intraformational breccia and calcareous siltstone; commonly highly fossiliferous.  Conformably overlies O'Hara Shale and Selwyn Range Limestone; interfingers with O'Hara Shale also.||||||02-APR-07
15420|Pomegranate Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, marl, breccia; minor chert.||||||
15420|Pomegranate Limestone|63450|5|Briefly described|p78 Fig. 5, p82|Late Cambrian|Late Cambrian|Conformably overlies Devoncourt Limestone. Max. thickness: 396m. Geological province: Georgina Basin, Burke River Structural Belt. Bituminous limestone, flaggy limestone, sandy limestone and intraformational breccia of shallow marine origin.||||||07-FEB-11
15420|Pomegranate Limestone|64068|3|Fully described|p70, 67, 69|Late Cambrian|Late Cambrian|Correlated with Arrinthrunga Formation, Georgina Limestone.||Of Narpa Group.||Conformably overlies  and laterally interdigitates with O'Hara Shale. Conformably overlain by Chatsworth Limestone.|Foetid calcimudstone, marly and quartzic limestone, marl, quartzic and intraclast grainstone, calcareous siltstone, chert, intraformational breccia.|04-APR-12
15420|Pomegranate Limestone|65489|6|Mentioned|p127|||Burke River Structural Belt, Georgina Basin. Little hydrocarbon potential: TOC at 0.16%.||||||
15420|Pomegranate Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Narpa Group.||Overlies Devoncourt Limestone and O'Hara Shale. Is overlain by Chatsworth Limestone.|Limestone, marl, breccia; minor chert.|
15420|Pomegranate Limestone|67870|5|Briefly described|p39, p43-46|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Part of a ~600m thick package with high amplitude discontinuous seismic reflections.||||||
15420|Pomegranate Limestone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Limestone, marl, breccia and minor chert|
15420|Pomegranate Limestone|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
15420|Pomegranate Limestone|69573|6|Mentioned|p659, 661|||Georgina Basin.||||||
15420|Pomegranate Limestone|69591|3|Fully described|p87, p92-94, p96-97|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Crops out between Limestone Creek (in the N) and Mistake Bore (in the S). 30m thick at the type area (on Pomegranate Creek); up to 120m elsewhere. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Resembles Devoncourt and Selwyn Range Limestones; distinguished by fossil content (named). [Relationship accounts with O'Hara Shale are contradictory.]||Narpa Group.||Overlies Devoncourt Limestone. Is overlain by Chatsworth Limestone and, gradationally, the O'Hara Shale (and interfingers with it).|Pink or grey, thinly laminated, silty and sandy calcilutite, marl with ellipsoidal lenses of limestone, dark bituminous limestones, common intraformational breccias and siliceous limestones with minor chert.|
15420|Pomegranate Limestone|72297|5|Briefly described|p747|||Georgina Basin. TOC values indicate this unit has one of the best source rock potentials in the Burke River Structural Belt.||||||
15420|Pomegranate Limestone|72321|6|Mentioned|Fig 2|Jiangshanian|Guzhangian|Burke River Structural Belt, Georgina Basin.  Australian stages: Mindyallan to Iverian.||of Narpa Group.||||
15420|Pomegranate Limestone|72358|6|Mentioned|117|||Of Georgina Basin.||||||
15420|Pomegranate Limestone|72516|6|Mentioned|p93|Furongian|Furongian|Eastern Georgina Basin. Age from equivalent relationship.||||Equivalent to the Arrinthrunga Formation.||07-JUN-21
15420|Pomegranate Limestone|73418|5|Briefly described|p4 Fig.3|Furongian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Overlies Selwyn Range Limestone|Limestone.|
15423|Pomona beds|23251|5|Briefly described|Table 1 p6|Tertiary|Tertiary|Age based on dicotyledon leaves. Pomona Basin.||||||30-NOV-05
15423|Pomona beds|41917|6|Mentioned|p522|||||||||
15423|Pomona beds|43077|5|Briefly described|p9|||||||||
15423|Pomona beds|43100|4|Described|p47|Tertiary|Tertiary|Early - Middle Tertiary age.||||||
15423|Pomona beds|44928|5|Briefly described|Map Legend||Tertiary|||||||
15423|Pomona beds|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott, Mueller and Poodyea Formations; Austral Downs, Horse Creek and Noranside Limestones; Mount Coley Sinter, and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
15423|Pomona beds|68679|6|Mentioned|p312|Neogene|Paleogene|Northern New England Orogen.||||||
15423|Pomona beds|69599|5|Briefly described|p586, p595|Cenozoic|Cenozoic|Bryan (1956) and others. Pomona Basin. Up to 30m thick. Age not determined; considered early-middle Cenozoic. RELATED UNITS (continued): Also correlated (at least partly) with Beaudesert, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek, Herbert Creek and Rossmoya beds.||||Unconformably overlies Landsborough Sandstone. Correlated (at least partly) with Flinders Dolomite; Oakdale Sandstone; Elliott, Petrie, Lowmead Formations; see COMMENTS for more.|Sandstone, shale and gravel with interbedded thin basalt flows in the N and NE. Extensively lateritised.|
15428|Poodyea Formation|22954|6|Mentioned|Fig3p9|||||||||
15428|Poodyea Formation|24442|6|Mentioned|p49|Cenozoic|Cenozoic|Fluviatile deposits.||||||
15428|Poodyea Formation|38832|2|Defined|p160|Tertiary|Tertiary|||||||
15428|Poodyea Formation|39495|6|Mentioned|p142|||||||||
15428|Poodyea Formation|39921|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
15428|Poodyea Formation|49027|4|Described|p22|||||||||
15428|Poodyea Formation|60122|5|Briefly described|p36|Cenozoic|Cenozoic|Cobble and boulder conglomerate, pebbly sandstone.  Unconformable on Nora Formation, Carlo Sandstone, Mithaka Formation and Ethabuka Sandstone. Max. thickness: 10m. Geol.Prov: Georgina Basin. See also p4-5, p10 Tb. 1.||||||19-NOV-08
15428|Poodyea Formation|60590|5|Briefly described|Map legend|Cenozoic|Cenozoic|Cobble and boulder conglomerate, pebbly sandstone.||||||19-NOV-08
15428|Poodyea Formation|61155|5|Briefly described|p16|Early Miocene|Early Miocene|Overlain by Mount Coley Sinter. Age: 21-17Ma. Thickness: 6m. Geological Province: Georgina Basin.||||||
15428|Poodyea Formation|61404|5|Briefly described|Map legend|Neogene||Cobble and boulder conglomerate, pebbly sandstone.  Geological Province: southern Georgina Basin.||||||
15428|Poodyea Formation|63450|5|Briefly described|p78 Fig. 5|Tertiary|Tertiary|Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
15428|Poodyea Formation|64068|3|Fully described|p79,p42, p ix|Miocene|Miocene|Proposed Radke (1983). Overlies Georgina Basin rocks. Formerly included in Cravens Peak beds (Reynolds in Smith 1965), Mithaka Formation, Carlo Sandstone (Smith 1965, and others).||||Unconformably overlies Cravens Peak beds, Ethabuka and Carlo Sandstones, Mithaka and Nora Formations.|Cobble and boulder conglomerate, pebbly sandstone. Fluviatile channel deposits.|04-APR-12
15428|Poodyea Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neogene|Paleogene|Age: Tertiary.|||||Boulder conglomerate, cross-stratified sandy conglomerate and pebbly sandstone.|
15428|Poodyea Formation|67870|6|Mentioned|p43|Cenozoic|Cenozoic|Georgina Basin.||||||
15428|Poodyea Formation|68553|6|Mentioned|Map legend|Neogene|Paleogene|This unit, as well as Elliott and Mueller Formations; Austral Downs, Horse Creek and Noranside Limestones; Mount Coley Sinter, Pomona beds and unnamed sedimentary units, are all mapped under the symbol, Tm.||||||
15428|Poodyea Formation|69458|5|Briefly described|p42:20|Neogene|Paleogene|Toko Syncline. Overlies SE Georgina Basin. 10m thick. Fluvial channel deposits. Pre-Quaternary Cenozoic age is likely; is overlain by Quaternary cover.||||Unconformably overlies Nora, Mithaka Formations; Carlo, Ethabuka Sandstones; Cravens Peak beds.|Sinuous outcrops of cobble and boulder conglomerate, cross-stratified conglomerate and pebbly sandstone. Some clasts are of the Carlo Sandstone.|14-SEP-18
15428|Poodyea Formation|69591|6|Mentioned|p96|||(Some?) rocks of this unit, along the Toomba Range SW of Boulia, were originally mapped as Cravens Peak beds.||||||
15428|Poodyea Formation|69599|5|Briefly described|p580, p584, p600|Miocene|Miocene|Radke et al. (1983). Straddles the QLD-NT border: occupies a series of small, discontinuous, linear outcrops in, and to the W and SW of, the Toko Range. Up to 10m thick. High-energy fluvial deposits. Age control is poor. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek, Noranside, Austral Downs Limestones.||||Unconformably overlies Nora and Mithaka Formations and Carlo and Ethabuka Sandstones. Correlated with Whitula and Doonbara Formations; Mount Coley Sinter; see COMMENTS for more.|Locally derived conglomerate and pebbly sandstone.|
15442|Poolowanna Formation|12597|5|Briefly described|p498-499, p501|||NW Eromanga Basin. 200m thick. Appears as Poolawanna Formation on p501.||||Grades laterally into, and is overlain by, Algebuckina Sandstone. Is conformably overlain by Hutton Sandstone.|Mainly fluvial sequence of interbedded fine-grained sub-labile sandstone, siltstone and mudstone, with minor coal seams generally <0.5m thick.|
15442|Poolowanna Formation|13497|5|Briefly described|p89, p104, p112, p114|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a high-sinuosity fluvial, overbank or lacustrine environment. Oil and gas reservoir. See also p115 fig 6.33, p119, p130, p138 fig 8.17, p141, p149-p151, p153,  p167, p170, p216.||||Overlies the Patchawarra Formation. Unconformably overlies the Tinchoo Formation. Disconformably overlain by the Cuddapan Formation.  Overlain by the Hutton Sandstone.|Sandstones, siltstone, shale and minor coal.|
15442|Poolowanna Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12, p172|Middle Jurassic|Early Jurassic|In Eromanga Basin.||||||
15442|Poolowanna Formation|22839|6|Mentioned|P33|||||||||
15442|Poolowanna Formation|22883|5|Briefly described|P31, Fig2||Early Jurassic|Overlying unit is Algebuckina Sandstone||||||
15442|Poolowanna Formation|23054|6|Mentioned|Fig5p22|Aalenian|Sinemurian|||||||
15442|Poolowanna Formation|23154|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Geological Province - Eromanga Basin.||||||
15442|Poolowanna Formation|23155|4|Described|p25|Early Jurassic|Early Jurassic|Early Jurassic in age from palynological evidence. Unit contains coal seams (<1m typically) and has carbonised plant fossils preserved on bedding surfaces.  On STRZELECKI the unit is overlain by Hutton Sandstone (conformity).||||||16-SEP-08
15442|Poolowanna Formation|23375|4|Described|Fig2 p265|Aalenian|Sinemurian|In the Eromanga Basin.||||||17-JAN-08
15442|Poolowanna Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24204|5|Briefly described|p266, 263 Fig.4, p266 Fig.7|Early Jurassic|Early Jurassic|Overlain unconformably by Algebuckina Formation. Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|24210|5|Briefly described|p132, p133 Fig. 2|Middle Jurassic|Early Jurassic|Comprises fluvial sandstones, interbedded with shales and discontinuous, thin coals. Geological Province: Eromanga Basin.||||||16-SEP-08
15442|Poolowanna Formation|24372|6|Mentioned|p21|||Geological Province: Cooper Basin.||||||
15442|Poolowanna Formation|24482|5|Briefly described|p44|||Geological Province: Eromanga Basin.||||||
15442|Poolowanna Formation|37776|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|40670|6|Mentioned|Fig.9|||||||||
15442|Poolowanna Formation|40926|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41060|6|Mentioned|p2|||See also Fig.5||||||
15442|Poolowanna Formation|41061|6|Mentioned|p20|||||||||
15442|Poolowanna Formation|41063|2|Defined|p46|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|41084|5|Briefly described|Fig.2|||||||||
15442|Poolowanna Formation|41175|6|Mentioned|Fig.1|||||||||
15442|Poolowanna Formation|41176|6|Mentioned|Table 2|||||||||
15442|Poolowanna Formation|41183|6|Mentioned|p310|||||||||
15442|Poolowanna Formation|41187|6|Mentioned|Fig.2|||||||||
15442|Poolowanna Formation|41216|6|Mentioned|p300|||||||||
15442|Poolowanna Formation|41724|6|Mentioned|p381|||||||||
15442|Poolowanna Formation|42008|5|Briefly described|p266|||||||||
15442|Poolowanna Formation|42357|6|Mentioned|p11|||||||||
15442|Poolowanna Formation|42463|6|Mentioned|Fig.4 P171|||||||||
15442|Poolowanna Formation|42520|5|Briefly described|p6|||||||||
15442|Poolowanna Formation|42746|4|Described|p10|||See also Fig.6.||||||17-JAN-08
15442|Poolowanna Formation|43052|5|Briefly described|Table 2.1|||||||||
15442|Poolowanna Formation|43628|6|Mentioned|Fig.3|Early Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|44133|4|Described|p105|Jurassic|Early Jurassic|Previously known as 'Cuttapirie beds', 'basal Hutton', and 'basal Jurassic'. Maximum Thickness in type section 206m. Intertongues with and is overlain by the Algebuckina Sandstone and Hutton Sandstone.||||||17-JAN-08
15442|Poolowanna Formation|60386|6|Mentioned|p299|Early Jurassic|Early Jurassic|Cooper/Eromanga Basin. Non-marine.||||||
15442|Poolowanna Formation|60717|5|Briefly described|p40 Fig. 2, p42|Middle Jurassic|Early Jurassic|Unconformity at base, over the Cuddapan Formation. Overlain by Hutton Sandstone. Geological Province: Eromanga Basin.||||||31-JAN-08
15442|Poolowanna Formation|61015|6|Mentioned|p44, p45|Early Jurassic|Early Jurassic|||||||19-APR-05
15442|Poolowanna Formation|61613|6|Mentioned|p282 Fig. 2|Middle Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|61614|6|Mentioned|p289, p297, p290 Fig. 2|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin. Contain coals and shales.||||||17-MAR-09
15442|Poolowanna Formation|61615|5|Briefly described|p302, p302 Fig. 2, p305, p306, p307|Middle Jurassic|Jurassic|Geological Province: Eromanga Basin. Comprises fluvial sandstones interbedded with shales and discontinuous, thin coals.||||||09-MAY-13
15442|Poolowanna Formation|62046|5|Briefly described|p125 Fig. 2|Jurassic|Jurassic|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
15442|Poolowanna Formation|62376|5|Briefly described|p84|Middle Jurassic|Late Triassic|Geological Province: Pedirka Basin.||||||09-FEB-10
15442|Poolowanna Formation|62537|6|Mentioned|p191 Fig.2, p192.|Middle Jurassic|Early Jurassic|Eromanga Basin. Significant hydrocarbon source potential.||||Is overlain by Hutton and Algebuckina Sandstones.||
15442|Poolowanna Formation|62730|5|Briefly described|p352 Fig. 1|Early Jurassic|Early Jurassic|Geological Province: Eromanga Basin.||||||14-APR-08
15442|Poolowanna Formation|63979|2|Defined|p32, Fig. 44|Toarcian|Pleinsbachian|Supersedes "Poolowanna beds". Unconformable on Cuddapan Fm; conformable below Hutton Sandstone. Max.thick: 165m.Comprises lower dominantly sandstone subunit + upper dominantly mudstone subunit - more lithology available.Geol. Prov.Eromanga Basin.||||||07-FEB-11
15442|Poolowanna Formation|64048|5|Briefly described|p64 Tb. 2, p69|||Geological Province: Eromanga Basin. Possesses hydrocarbon source potential.||||||07-FEB-11
15442|Poolowanna Formation|64197|6|Mentioned|p625 Fig.1c|Early Jurassic|Early Jurassic|Overlies the Nappamerri Unconformity.||||Underlies the Hutton Sandstone.||
15442|Poolowanna Formation|64232|5|Briefly described|p12|Jurassic|Jurassic|Geological Province: Eromanga Basin. Coal occurs in deeper parts of the basin in this unit.||||||24-JUL-08
15442|Poolowanna Formation|64665|5|Briefly described|p53 Fig.2, p61.|Early Jurassic|Early Jurassic|Eromanga Basin. Lateral equivalent of Precipice Sandstone and Evergreen Formation in the Surat Basin. Hosts thin (to 0.5 m thick) uneconomic coal seams.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|64778|6|Mentioned|p13, 21, 28|Jurassic|Jurassic|Pedirka and Simpson Desert Basins. Appears as Poolawanna Formation on p13.  Potential hydrocarbon source.||||Is overlain by Algebuckina Formation.||
15442|Poolowanna Formation|65238|5|Briefly described|p3, p7 Fig. 8|Jurassic|Jurassic|Overlies Purni Formation. Geological province: Eromanga Basin. Meandering and anastomosing fluvial-floodplain deposits. See also p10, p14 Fig. 17.||||||16-FEB-10
15442|Poolowanna Formation|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlain by Hutton Sandstone.||||||08-MAR-12
15442|Poolowanna Formation|65489|5|Briefly described|p15, p24, p26, p45, p47,p49, p53, p55-62|Early Jurassic|Early Jurassic|See also p91, p96, p137, p151-152, p154-160. Eromanga Basin. 130-290m thick. Hydrocarbon source rock. Stratigraphic and structural trapping of Permian generated oil. Gas and oil reservoir accounting for 6.3% and 5% respectively of the Basin's production. Intraformational shale seal.||||Overlies Cuddapan Formation unconformably. Is overlain by Algebuckina Sandstone.|Includes meandering fluvial sandstones and organic-rich shales.|
15442|Poolowanna Formation|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded sandstone, ripple cross laminated; dark grey siltstone; shale; coal seams and breccias.|
15442|Poolowanna Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina Sandstone and Hutton Sandstone.||
15442|Poolowanna Formation|66915|5|Briefly described|p6 Fig.3|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|67323|5|Briefly described|p87-88, p95 Fig.12.5|Early Jurassic|Early Jurassic|Eromanga/Galilee Basins. Hydrocarbon exploration target in the Eromanga Basin.||||Is overlain by Hutton Sandstone.||
15442|Poolowanna Formation|67402|6|Mentioned|p114 fig ERO13, p117|||Seel also the Poolowanna Formation, Lower and Poolowanna Formation, Upper.||||||
15442|Poolowanna Formation|68731|6|Mentioned|p208, pp209-211|Jurassic|Jurassic|See also Poolawanna Formation.||||Unconformably overlies Tinchoo Formation (Nappamerri Group).||17-JUL-14
15442|Poolowanna Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
15442|Poolowanna Formation|69019|5|Briefly described|p85 Fig.21.|Early Jurassic|Early Jurassic|Southern Eromanga Basin.||||Is overlain by Algebuckina and Hutton Sandstones.||
15442|Poolowanna Formation|69023|6|Mentioned|p86, p89 Fig.20, p90|Middle Jurassic|Early Jurassic|||||||
15442|Poolowanna Formation|69454|5|Briefly described|p38:3, 7 Fig.38.6; 38:12-13, 14 Fig.38.9|Early Jurassic|Early Jurassic|Eromanga Basin. Sandstones have fair to good reservoir potential, sealed by intra-formational shales.||||Unconformably overlies Peera Peera Formation. Is overlain by Algebuckina Sandstone.||12-JUL-16
15442|Poolowanna Formation|69457|4|Described|p41:2-4; 41:5 Fig.41.4; 41:15-17|Early Jurassic|Early Jurassic|Moore (1986); formerly Poolowanna beds of Wiltshire (1978). Eromanga Basin; entirely subsurface. 205m thick; thins to the W. Fluvial and lacustrine deposits. Pliensbachian-Toarcian age. The coal is black, dull and shaly and the thin (0.5m thick) seams are uneconomic. Contains confirmed oil source rocks with TOCs up to 15%. Thermal maturity, prospects and leads discussed in some detail. Lacustrine shales might form a regional seal. Contains the deepest reservoir units in the Eromanga Basin succession.||||Unconformably overlies Cuddapan Formation. Is overlain conformably by/intertongues with Hutton Sandstone and Algebuckina Sandstone. Lateral equivalent of Precipice Sandstone and Evergreen Formation.|Sandstone, siltstone and coaly shale, arranged in two upward-fining cycles. Thin discontinuous coal seams.|12-JUL-16
15442|Poolowanna Formation|69582|6|Mentioned|p65|Early Jurassic|Early Jurassic|Eromanga Basin.||||Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|69594|4|Described|p519, p524, p526, p531-532, p535, p545|Early Jurassic|Early Jurassic|See also p572. Eromanga Basin. Originally defined in the Poolowanna Trough in SA (Wiltshire, 1978; Moore, 1986); the type section is in DIO Poolowanna 1. Maximum thickness is 165m. Represents cyclic fluvio-lacustrine deposition. Palynofloras in QLD are Pliensbachian-Toarcian and are generally correlated with those of upper Precipice Sandstone-Evergreen Formation. Is a minor hydrocarbon reservoir; has hydrocarbon source potential. RELATED UNITS (continued): Passes laterally into Precipice Sandstone. Equivalent to Evergreen Formation.||||Unconformably overlies Cuddapan, Tinchoo, Toolachee and Patchawarra Formations. Is overlain conformably by Hutton Sandstone (and intertongues with it) and Algebuckina Sandstone. See COMMENTS for more.||
15442|Poolowanna Formation|69633|6|Mentioned|p14|||Eromanga Basin.||||||
15442|Poolowanna Formation|69673|5|Briefly described|p154, p154 fig 126, p159, p160, p161|Jurassic|Jurassic|Up to 205m thick. Confirmed oil source rock.||||Unconformably (or disconformably) overlain by Algebuckina Sandstone, Hutton Sandstone, overlies Walkandi Formation, unconformably overlies Peera Peera Formation|Interbedded sandstone that fines upwards into coaly shale and siltstone.|
15442|Poolowanna Formation|69790|6|Mentioned|p1063 Fig.2|Early Jurassic|Early Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|69797|5|Briefly described|p17 incl Fig.2|Middle Jurassic|Early Jurassic|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are the highly carbonaceous shales of Poolowanna Formation, the coals and carbonaceous shales of Birkhead Formation, and organic-rich shales and siltstones of Murta Formation. Age approximated from figure. Geol. Prov: Eromanga Basin.||||||17-JAN-17
15442|Poolowanna Formation|69946|3|Fully described|p10-11, p51, p57-60, p74-82|Middle Jurassic|Early Jurassic|Eromanga Basin. Moore (1986); formerly Poolowanna beds (Wiltshire, 1978). Type section remains that of Wiltshire (1978), viz. the interval 2387 - 2593m in Poolowanna 1; not the interval 2422-2476m in Cuttapirrie 1 which has also been called Poolowanna Formation and 'Cuttapirrie beds' in SA. Up to 205m thick. Wireline log correlations.||||Intertongues with, and is overlain by, Algebuckina and Hutton Sandstones.|Interbedded grey to brown carbonaceous siltstone; pale grey to buff, very fine- to medium-grained sandstone; rare coal seams.|
15442|Poolowanna Formation|69947|5|Briefly described|p3-5, p13 Fig.7.2, p16-21 Figs.7.5-10|Early Jurassic|Early Jurassic|See also p23 Fig.7.12. Eromanga Basin. First deposits above the basal Eromanga Basin unconformity. Amalgamated channel sands and infilled palaeovalleys; no laterally extensive sand sheets. Facies described in some detail.||||Unconformably overlies Cuddapan Formation. Is overlain by Hutton Sandstone.|Sandstone, minor shale and thin coal seams.|
15442|Poolowanna Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Unconformably overlies Peera Peera and Purni Formations. Is overlain by Algebuckina Sandstone.||
15442|Poolowanna Formation|69982|6|Mentioned|p49-50|Early Jurassic|Early Jurassic|The Sturt 7 oil well was re-perforated in this unit after extracting Mooracoochie Volcanics oil, extending production by almost one-half.||||||
15442|Poolowanna Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Jurassic|Early Jurassic|Eromanga Basin. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments. Up to 130m thick. This unit forms a source rock that hosts an oil and gas discovery.||||Unconformably overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.|Sandstone, siltstone, shale and coal.|
15442|Poolowanna Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Cuddapan Formation. Overlain by the Hutton Sandstone.||
15442|Poolowanna Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Peera Peera Formation. Overlain by the Algebuckina Sandstone.||24-OCT-19
15442|Poolowanna Formation|71342|3|Fully described|Ch 1 p3, Ch4 p25,  Ch5 p10-p12, Ch5 p30|Aalenian|Hettangian|Eromanga Basin. Source of significant production of gas in the Eromanga Basin. Originally the Poolowanna beds of Wiltshire (1978) before being raised to formation status by Moore (1986). This unit has also been previously referred to as the 'basal Hutton Sandstone', 'Cuttapirrie beds' (in South Australia or as the 'basal Jurassic' (in Queensland). A type section is mentioned in Poolowanna 1. Petrography is discussed in some detail. Spore-pollen zone is given in Ch5 p57. Reaches a maximum thickness of 205m in Poolowanna 1. Interpreted to have been deposited in fluvial channels meandering across a floodplain with minor coal swamps. Sequence stratigraphy discussed in detail (Ch7) as is source rock potential and hydrocarbon geochemistry (Ch8). See also Ch5 p51, Ch5 p57-p59, Ch5 p74, Ch6 p5-p6, Ch7 p3-p5, Ch7 p10, Ch7 p13, Ch7 p16-p17, Ch7 p20, Ch8 p2, Ch8 p8, Ch8 p10-p11, Ch9 p5, Ch9 p11, Ch9 p18, Ch10 p3, Ch10 tbl 10.1, Ch10 p6, Ch10 p14, Ch10 p17, Ch11 p2, Ch11 p7-p8, Ch11 p13, Ch12 p2p3, Ch12 tbl 12.1, Ch12 p6, Ch12 p9, Ch12 p11-p14, Ch13 p3, Ch13 p8, Ch14 p2-p7.||||Unconformably overlies the Peera Peera and Cuddapan Formations. Overlain by the Algebuckina and Hutton sandstones.|Interbedded carbonaceous siltstone, sandstone and rare coal seams. Sandstones range from very fine to medium grained and contain minor pebbles and granules of quartzite and reworked basement.|
15442|Poolowanna Formation|71805|5|Briefly described|p75-p76|Toarcian|Pleinsbachian|Eromanga Basin. This unit is temporally equivalent to the Precipice Sandstone.||||Overlain by the Hutton Sandstone.||16-MAY-19
15442|Poolowanna Formation|71863|5|Briefly described|p4|||Eromanga Basin. Potential petroleum source (although the majority is derived from the underlying Cooper Basin units).||||||
15442|Poolowanna Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with source rock potential.||||||
15442|Poolowanna Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD).||||Unconformably overlies Nappamerri Group. Is overlain by Algebuckina, Hutton Sandstones.||
15442|Poolowanna Formation|72476|6|Mentioned|p36 Fig.9, p37|||Eromanga Basin. Time-temperature thermal history diagram. Only <1 km thickness preserved.||||||
15442|Poolowanna Formation|73167|6|Mentioned|p664 Fig. 2|Jurassic|Jurassic|Eromanga Basin. Contains oil.||||||
15442|Poolowanna Formation|73249|6|Mentioned|p319|Cretaceous|Jurassic|Eromanga Basin.||||||
15442|Poolowanna Formation|73251|6|Mentioned|p49, p55-56, p62|Early Jurassic|Early Jurassic|Eromanga Basin. Meandering-anastomosing fluvial depositional setting. Hydrocarbon source rock that contains[?] gas and oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73281|6|Mentioned|p1, Appendix (DIP)|Early Jurassic|Early Jurassic|Eromanga Basin. Petroleum source rocks. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Poolowanna Formation, lower.||||||
15442|Poolowanna Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Overlain by Hutton Sandstone.||
15442|Poolowanna Formation|73479|5|Briefly described|p156 Fig.2, p159, p179|Jurassic|Jurassic|Eromanga Basin. Fluvial depositional environment.|ca 200-180 Ma|||Unconformably overlies Cuddapan Formation, underlies Hutton Sandstone||
15450|Poperima Formation|29728|6|Mentioned|p394|||||||||
15450|Poperima Formation|30451|4|Described|p31|||See also P32||||||
15450|Poperima Formation|30668|6|Mentioned|p582|||Occurrence of Septatopora pustulosa (Crockford).||||||
15450|Poperima Formation|30772|6|Mentioned|p5|||Fauna||||||
15450|Poperima Formation|31659|6|Mentioned|p58|||||||||
15450|Poperima Formation|32141|6|Mentioned|p152|||||||||
15450|Poperima Formation|32868|6|Mentioned|p202|||||||||
15450|Poperima Formation|33774|6|Mentioned|p23|||Stratigraphy||||||
15450|Poperima Formation|33992|6|Mentioned|p238|||M.Carb.  See also P237||||||
15450|Poperima Formation|34085|6|Mentioned|Cor.chart|||Westphalian||||||
15450|Poperima Formation|34086|6|Mentioned|p264|||||||||
15450|Poperima Formation|35492|6|Mentioned|p145|||||||||
15450|Poperima Formation|36296|6|Mentioned|p148|||||||||
15450|Poperima Formation|39445|5|Briefly described|Table 7 p98|||||||||
15450|Poperima Formation|42547|5|Briefly described|p52|||||||||
15450|Poperima Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
15450|Poperima Formation|43983|14|Not recorded|p1,3,8,11,14|||||||||
15450|Poperima Formation|44091|14|Not recorded|p37,Tb.3,p47||Early Carboniferous|Middle Carb.||||||
15450|Poperima Formation|44360|2|Defined|p1-3,16-19,21,23,27||Westphalian|p28,30-32,35,map. Unit of Boiling Creek Group.||||||
15450|Poperima Formation|44369|2|Defined|p169-171|||||||||
15450|Poperima Formation|44370|14|Not recorded|p219,Tb.7|||||||||
15450|Poperima Formation|44372|6|Mentioned|p5,6,11||Early Carboniferous|Overlies Branch Creek Formation. Underlies Rands Formation. (Middle Carboniferous)||||||
15450|Poperima Formation|44515|2|Defined|p30|||||||||
15450|Poperima Formation|44874|14|Not recorded|p102|||||||||
15450|Poperima Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
15450|Poperima Formation|68008|5|Briefly described|p120|Late Carboniferous|Late Carboniferous|Maxwell (1959, 1960, 1964). Yarrol and Cannindah areas. Subsequently subsumed into the Lorray Formation.||Boiling Creek Group.||||
15450|Poperima Formation|68679|5|Briefly described|p341|||Maxwell (1960). Cannindah area. Superseded; assigned to Boiling Creek Group by McKellar (1967) which itself is (?being) replaced by Lorray Formation.||Boiling Creek Group.||||
15464|Port Clinton Granite|48915|6|Mentioned|p26|||See also p27.||||||11-MAY-18
15488|Portal Creek Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
15488|Portal Creek Volcanics|40896|6|Mentioned|p51|||||||||
15488|Portal Creek Volcanics|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
15488|Portal Creek Volcanics|44707|14|Not recorded|p3|||Ref. to Stephenson 1956.(unpubl)||||||
15488|Portal Creek Volcanics|44786|14|Not recorded|p193-202|Late Triassic|Middle Triassic|||||||
15488|Portal Creek Volcanics|48917|6|Mentioned|p7|||Refers Stephenson (1954,1956,1959)||||||
15488|Portal Creek Volcanics|66855|6|Mentioned|p955.|||||||||
15488|Portal Creek Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Aranbanga and North Arm Volcanic Groups; the Agnes Water, Bobby, Chillingham, Coulston, Dangore, Dooloo Tops, Morang, Mount Byron, Mount Eagle, Ooramera, and Winterbourne Volcanics; the Brisbane Tuff, Cynthia beds, and the Callide Coal Measures, are all mapped under the symbol, Rvs.||||||
15530|Poyungan beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
15530|Poyungan beach sand|39495|6|Mentioned|p142|||||||||
15530|Poyungan beach sand|62102|5|Briefly described|p367 Tb. 1|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast - forms a coastal strandplain.  Age: 335Ka.||||||
15540|Precipice Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498|Early Jurassic|Early Jurassic|N Surat and Mulgildie Basins. 40-150m thick in Surat Basin; 60-150m thick in Mulgildie Basin.|||||Mainly quartzose sandstone, becoming finer upwards with minor siltstone bands.|
15540|Precipice Sandstone|13516|5|Briefly described|p159 fig 8, p163, 166,167, 168, 169 p139|Early Jurassic|Early Jurassic|From Callide Basin, Surat Basin, Eromanga Basin. Age of base varies across Surat Basin.||||||
15540|Precipice Sandstone|22482|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|22757|5|Briefly described|Table6,p12|Early Jurassic|Early Jurassic|200 m.||||||
15540|Precipice Sandstone|22865|4|Described|p295,Table22.1p296-7|Sinemurian|Early Jurassic|||||||
15540|Precipice Sandstone|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22976|5|Briefly described|p42 Fig.4|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22977|5|Briefly described|p67 Fig.2|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22981|5|Briefly described|p259|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|23037|5|Briefly described|p34,117||Jurassic|Underlain by Torsdale Volcanics.||||||14-FEB-07
15540|Precipice Sandstone|23050|5|Briefly described|p9 Fig.2, 17|Jurassic|Jurassic|of Surat Basin.||||||
15540|Precipice Sandstone|23053|6|Mentioned|Fig10p17|Sinemurian||||||||
15540|Precipice Sandstone|23056|6|Mentioned|8 table 1A|||||||||
15540|Precipice Sandstone|23425|6|Mentioned|p391.|||||||||
15540|Precipice Sandstone|23799|3|Fully described|p50, p10 Tb. 1|Early Jurassic|Early Jurassic|Part of this group was previously mapped as Marburg Subgroup.  See also p48 Fig. 3.  Overlain by Evergreen Formation; unconformably overlies parts of Chahpingah Meta-Igneous and Boondooma Igneous Complexes.   Max. thickness: >50m.Geol. Prov: Surat Basin.||||||
15540|Precipice Sandstone|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
15540|Precipice Sandstone|23841|5|Briefly described|p448|Early Jurassic|Early Jurassic|Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Early Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
15540|Precipice Sandstone|23982|5|Briefly described|p35 Fig. 7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|24068|4|Described|p269|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.  Maximum thickness: 180m.||||||
15540|Precipice Sandstone|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|24159|5|Briefly described|p148 Fig.2, p151|Early Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Evergreen Formation. Underlying Unit: unconformity with Moolayember Formation.||||||
15540|Precipice Sandstone|24236|5|Briefly described|p364|Jurassic|Jurassic|Overlies Callide Coal Measures. Geological Province: Callide Basin.||||||
15540|Precipice Sandstone|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24489|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24491|5|Briefly described|p12|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24615|5|Briefly described|CD|Jurassic|Jurassic|[Jp].  Thick-bedded, cross-bedded, fine- to coarse-grained pebbly quartzose sandstone, and minor lithic sublabile sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|29385|6|Mentioned|p80|||Other references on P81,82. Jurassic.||||||
15540|Precipice Sandstone|29387|6|Mentioned|p30|||See also Table 5.||||||
15540|Precipice Sandstone|29389|6|Mentioned|p19|||Early Jurassic.||||||
15540|Precipice Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
15540|Precipice Sandstone|29394|6|Mentioned|p145|||||||||
15540|Precipice Sandstone|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
15540|Precipice Sandstone|29411|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|29532|6|Mentioned|p15|||||||||
15540|Precipice Sandstone|29537|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|29539|6|Mentioned|p8|||Drilling.||||||
15540|Precipice Sandstone|29540|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|29541|6|Mentioned|p9|||Drilling.||||||
15540|Precipice Sandstone|29591|6|Mentioned|p69|||||||||
15540|Precipice Sandstone|29721|6|Mentioned|p76|||||||||
15540|Precipice Sandstone|29961|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|29964|6|Mentioned|p5|||Jurassic||||||
15540|Precipice Sandstone|29967|6|Mentioned|p118|||||||||
15540|Precipice Sandstone|30102|6|Mentioned|p17|||Correlation with basal Hutton Sandstone.||||||
15540|Precipice Sandstone|30103|6|Mentioned|p10|||||||||
15540|Precipice Sandstone|30232|4|Described|p667,668,672-679||Early Jurassic|||||||
15540|Precipice Sandstone|30451|3|Fully described|p70|||See alsp p71. Early Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30455|6|Mentioned|p5|||See also P13. Jurassic age||||||
15540|Precipice Sandstone|30456|6|Mentioned|p95|||||||||
15540|Precipice Sandstone|30457|6|Mentioned|p96|||||||||
15540|Precipice Sandstone|30458|6|Mentioned|p3|||Jurassic age||||||
15540|Precipice Sandstone|30460|6|Mentioned|p5|||See also P13. Jurassic age||||||
15540|Precipice Sandstone|30462|6|Mentioned|p356|||||||||
15540|Precipice Sandstone|30464|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|30465|6|Mentioned|p4|||||||||
15540|Precipice Sandstone|30466|6|Mentioned|p40|||See also P5. Jurassic age||||||
15540|Precipice Sandstone|30469|6|Mentioned|p273|||||||||
15540|Precipice Sandstone|30471|6|Mentioned|p131|||||||||
15540|Precipice Sandstone|30472|6|Mentioned|p132|||Pollen distribution||||||
15540|Precipice Sandstone|30474|6|Mentioned|p249|||Proposed to include upper sandstone sequence of Callide Coal Measures.||||||
15540|Precipice Sandstone|30475|6|Mentioned|p168|||||||||
15540|Precipice Sandstone|30508|6|Mentioned|p91|||Productive formation||||||
15540|Precipice Sandstone|30691|4|Described|p6|||See also p15,19,20,21,Table 4. Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30695|4|Described|Table 3|||Lower Jurassic age||||||
15540|Precipice Sandstone|30696|4|Described|Table 4|||Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30699|6|Mentioned|p53|||Early Jurassic age||||||
15540|Precipice Sandstone|30700|6|Mentioned|p22|||Map. Lower Jurassic age||||||
15540|Precipice Sandstone|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30702|6|Mentioned|Fig.1|||See Stratigraphic Table||||||
15540|Precipice Sandstone|30854|4|Described|Table 4|||Lower Jurassic age||||||
15540|Precipice Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|30915|6|Mentioned|p98|||||||||
15540|Precipice Sandstone|30916|6|Mentioned|p98|||On table||||||
15540|Precipice Sandstone|31115|6|Mentioned|p32|||||||||
15540|Precipice Sandstone|31116|4|Described|p20|||See also p10. Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|31117|5|Briefly described|p379|||Lithology. Jurassic||||||
15540|Precipice Sandstone|31118|6|Mentioned|p311|||Part of Bundamba Gp. by Whitehouse (1954)||||||
15540|Precipice Sandstone|31120|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|31304|5|Briefly described|p628|||Lithology in drill hole.||||||
15540|Precipice Sandstone|31305|6|Mentioned|Fig. 1|||||||||
15540|Precipice Sandstone|31369|4|Described|p40|||See also p41-44. L.Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|31398|6|Mentioned|p268|||L.Jurassic.||||||
15540|Precipice Sandstone|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|31656|6|Mentioned|p8|||Unconformable on Clematis Sst.||||||
15540|Precipice Sandstone|31659|6|Mentioned|p74|||L.Jurassic||||||
15540|Precipice Sandstone|32038|4|Described|p428|||See also p429, 437. Early Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|32039|6|Mentioned|p115|||L.Jurassic. See also P119,120.||||||
15540|Precipice Sandstone|32040|6|Mentioned|p885|||Stratigraphic sequence||||||
15540|Precipice Sandstone|32136|6|Mentioned|p1|||Refers Reiser & Williams (1969)||||||
15540|Precipice Sandstone|32137|6|Mentioned|p357|||||||||
15540|Precipice Sandstone|32182|4|Described|p1|||Jurassic||||||
15540|Precipice Sandstone|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32276|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32496|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32712|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|32715|6|Mentioned|p1186|||Oil||||||
15540|Precipice Sandstone|32797|4|Described|Table 4|||L.Jur.||||||
15540|Precipice Sandstone|33059|4|Described|p311|||L.Jur.||||||
15540|Precipice Sandstone|33071|4|Described|p6|||L.Jur.||||||
15540|Precipice Sandstone|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33088|4|Described|Table 3|||L.Jur.||||||
15540|Precipice Sandstone|33090|4|Described|Table 4|||L.Jur.||||||
15540|Precipice Sandstone|33091|6|Mentioned|p10|||Stratigraphy||||||
15540|Precipice Sandstone|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33192|6|Mentioned|p21|||||||||
15540|Precipice Sandstone|33367|5|Briefly described|Table 1|||||||||
15540|Precipice Sandstone|33381|6|Mentioned|Table 1|||L.Jur.||||||
15540|Precipice Sandstone|33449|6|Mentioned|p6|||L.Jur.||||||
15540|Precipice Sandstone|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33530|5|Briefly described|Table 1|||Lower Jur.||||||
15540|Precipice Sandstone|33639|6|Mentioned|p10|||||||||
15540|Precipice Sandstone|33672|6|Mentioned|p41|||||||||
15540|Precipice Sandstone|33673|4|Described|p291|||||||||
15540|Precipice Sandstone|33675|4|Described|p412|||Lithology.||||||
15540|Precipice Sandstone|33774|3|Fully described|p46|||See also p24||||||14-FEB-07
15540|Precipice Sandstone|33971|6|Mentioned|p41|||Petroleum. Surat Basin.||||||
15540|Precipice Sandstone|34061|6|Mentioned|p54|||||||||
15540|Precipice Sandstone|34133|6|Mentioned|p1|||See also PP3,4,28. Jurassic.||||||
15540|Precipice Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic.||||||
15540|Precipice Sandstone|34172|6|Mentioned|p53|||Jurassic.||||||
15540|Precipice Sandstone|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|34212|6|Mentioned|p1|||Jurassic. See also PP2,3,4,5,etc.||||||
15540|Precipice Sandstone|34254|6|Mentioned|p481, p489|||Early Jurassic||||||
15540|Precipice Sandstone|34287|6|Mentioned|p170|||Jurassic. See also P173||||||
15540|Precipice Sandstone|34452|6|Mentioned|p1|||L.Jurassic. Palynology. See also PP2,3,4 etc||||||
15540|Precipice Sandstone|34613|4|Described|Table 4|||||||||
15540|Precipice Sandstone|35079|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|35148|4|Described|p415|||See also Table 1 and Fig.1.||||||
15540|Precipice Sandstone|35157|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|35560|6|Mentioned|p288|||||||||
15540|Precipice Sandstone|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
15540|Precipice Sandstone|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
15540|Precipice Sandstone|35811|5|Briefly described|Table 5|||||||||
15540|Precipice Sandstone|35901|6|Mentioned|p17|||||||||
15540|Precipice Sandstone|35937|6|Mentioned|Fig.5|||||||||
15540|Precipice Sandstone|36103|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|36111|6|Mentioned|p34|||||||||
15540|Precipice Sandstone|36233|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|36235|3|Fully described|p181|||See also Fig.1.||||||
15540|Precipice Sandstone|36236|6|Mentioned|p183|||||||||
15540|Precipice Sandstone|36243|6|Mentioned|p74|||See also Table 6A.||||||
15540|Precipice Sandstone|36331|6|Mentioned|p3|||See also P24, 31, 53||||||
15540|Precipice Sandstone|36333|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|36570|6|Mentioned|p26, p55|||See also Table 1.||||||
15540|Precipice Sandstone|36739|6|Mentioned|p4|||||||||
15540|Precipice Sandstone|36751|6|Mentioned|p387|||||||||
15540|Precipice Sandstone|36825|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|36905|4|Described|p17|||||||||
15540|Precipice Sandstone|36917|6|Mentioned|p151|||||||||
15540|Precipice Sandstone|36926|6|Mentioned|p176|||||||||
15540|Precipice Sandstone|37117|5|Briefly described|p313|||||||||
15540|Precipice Sandstone|37119|5|Briefly described|p318|||||||||
15540|Precipice Sandstone|37288|6|Mentioned|p41|||||||||
15540|Precipice Sandstone|37463|6|Mentioned|p483|||||||||
15540|Precipice Sandstone|37705|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|37749|6|Mentioned|p194|||||||||
15540|Precipice Sandstone|37995|4|Described|p62|||||||||
15540|Precipice Sandstone|37996|4|Described|p71|||||||||
15540|Precipice Sandstone|38064|6|Mentioned|42|||||||||
15540|Precipice Sandstone|38067|6|Mentioned|p59|||||||||
15540|Precipice Sandstone|38226|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|38358|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|38801|6|Mentioned|p129|||||||||
15540|Precipice Sandstone|39070|4|Described|p362|||||||||
15540|Precipice Sandstone|39212|4|Described|p15|||p24 petroleum reservoir. p25 aquifer. See alsopP37.||||||14-FEB-07
15540|Precipice Sandstone|39315|6|Mentioned|Fig.5|||||||||
15540|Precipice Sandstone|39445|5|Briefly described|Table 10|||||||||
15540|Precipice Sandstone|39478|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|39494|6|Mentioned|p137|||||||||
15540|Precipice Sandstone|39632|6|Mentioned|p209|||||||||
15540|Precipice Sandstone|39815|6|Mentioned|p444|||||||||
15540|Precipice Sandstone|39907|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|39943|6|Mentioned|Table 8A|||||||||
15540|Precipice Sandstone|40030|6|Mentioned|p135|||||||||
15540|Precipice Sandstone|40090|6|Mentioned|p83|||||||||
15540|Precipice Sandstone|40094|6|Mentioned|p23|||||||||
15540|Precipice Sandstone|40115|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|40120|6|Mentioned|p429|||||||||
15540|Precipice Sandstone|40121|6|Mentioned|p446|||||||||
15540|Precipice Sandstone|40245|6|Mentioned|Table 2|||||||||
15540|Precipice Sandstone|40249|6|Mentioned|p38|||||||||
15540|Precipice Sandstone|40250|4|Described|p29|||||||||
15540|Precipice Sandstone|40539|6|Mentioned|Fig.2|||||||||
15540|Precipice Sandstone|40540|6|Mentioned|p150|||||||||
15540|Precipice Sandstone|40541|3|Fully described|p108|||||||||
15540|Precipice Sandstone|40544|6|Mentioned|p161|||||||||
15540|Precipice Sandstone|40623|5|Briefly described|p72|||||||||
15540|Precipice Sandstone|40666|4|Described|p355|||||||||
15540|Precipice Sandstone|40675|6|Mentioned|Table 8A|||||||||
15540|Precipice Sandstone|40687|6|Mentioned|Table 3|||||||||
15540|Precipice Sandstone|40767|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|40832|3|Fully described|p254|||||||||
15540|Precipice Sandstone|41060|6|Mentioned|p2|||See also Fig.3||||||
15540|Precipice Sandstone|41061|6|Mentioned|p19|||||||||
15540|Precipice Sandstone|41064|6|Mentioned|p60|||||||||
15540|Precipice Sandstone|41097|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|41159|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|41177|6|Mentioned|Fig.2|||||||||
15540|Precipice Sandstone|41187|6|Mentioned|p217|||||||||
15540|Precipice Sandstone|41188|5|Briefly described|p232|||||||||
15540|Precipice Sandstone|41198|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|41210|6|Mentioned|p157|||||||||
15540|Precipice Sandstone|41211|6|Mentioned|p181|||||||||
15540|Precipice Sandstone|41216|6|Mentioned|p305|||||||||
15540|Precipice Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
15540|Precipice Sandstone|41247|6|Mentioned|p127|||||||||
15540|Precipice Sandstone|41266|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|41725|6|Mentioned|p400|||||||||
15540|Precipice Sandstone|41893|6|Mentioned|p514|||||||||
15540|Precipice Sandstone|41992|4|Described|Fig.2 P183|||||||||
15540|Precipice Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
15540|Precipice Sandstone|42067|4|Described|Apendix 2|||See also p311||||||14-FEB-07
15540|Precipice Sandstone|42250|6|Mentioned|p28|||||||||
15540|Precipice Sandstone|42370|5|Briefly described|Fig.3 P317|||||||||
15540|Precipice Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
15540|Precipice Sandstone|42493|5|Briefly described|p17, Fig.1 p18|||||||||
15540|Precipice Sandstone|42547|5|Briefly described|p46|||Jurassic.||||||
15540|Precipice Sandstone|42618|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|42634|6|Mentioned|p12|||Jurassic.||||||
15540|Precipice Sandstone|42865|6|Mentioned|p18|||||||||
15540|Precipice Sandstone|42911|5|Briefly described|p13|||||||||
15540|Precipice Sandstone|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
15540|Precipice Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
15540|Precipice Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
15540|Precipice Sandstone|43108|5|Briefly described|p34|||||||||
15540|Precipice Sandstone|43185|6|Mentioned|6||Jurassic|||||||
15540|Precipice Sandstone|43462|14|Not recorded|p15|||||||||
15540|Precipice Sandstone|43582|6|Mentioned|Fig.5,p16||Early Jurassic|||||||
15540|Precipice Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
15540|Precipice Sandstone|43714|6|Mentioned|Fig.3,p5||Early Jurassic|||||||
15540|Precipice Sandstone|43851|14|Not recorded|Tb p106,111||Early Jurassic|||||||
15540|Precipice Sandstone|43878|14|Not recorded|p85,86|||||||||
15540|Precipice Sandstone|43883|14|Not recorded|p18,19,21|||||||||
15540|Precipice Sandstone|43910|14|Not recorded|p5,19,20|||Correlated with Bundamba Group.||||||
15540|Precipice Sandstone|43912|14|Not recorded|p2,4,5,7|||||||||
15540|Precipice Sandstone|43915|14|Not recorded|p179|||||||||
15540|Precipice Sandstone|43916|14|Not recorded|p2479,2481||Jurassic|||||||
15540|Precipice Sandstone|43923|6|Mentioned|p1||Early Jurassic|||||||
15540|Precipice Sandstone|43924|14|Not recorded|p1,2,15||Lias|(Liassic)||||||
15540|Precipice Sandstone|43925|14|Not recorded|p31,37,48-50,Figs3,4|||||||||
15540|Precipice Sandstone|43960|14|Not recorded|p9,12||Jurassic|||||||
15540|Precipice Sandstone|43977|14|Not recorded|p576|||||||||
15540|Precipice Sandstone|43982|14|Not recorded|Map Legend|||||||||
15540|Precipice Sandstone|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|43993|14|Not recorded|p94,95,102|||Ref. to Whitehouse 1955. Equivalent to Helidon Sandstone.||||||
15540|Precipice Sandstone|43994|14|Not recorded|Map Legend|||||||||
15540|Precipice Sandstone|43995|14|Not recorded|p57,58|||Part of Bundamba Group.||||||
15540|Precipice Sandstone|43997|14|Not recorded|p114|||||||||
15540|Precipice Sandstone|43998|4|Described|p14,17,map||Early Jurassic|||||||
15540|Precipice Sandstone|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
15540|Precipice Sandstone|44026|14|Not recorded|p122,123|||||||||
15540|Precipice Sandstone|44028|14|Not recorded|Fig.2,p512||Jurassic|||||||
15540|Precipice Sandstone|44031|14|Not recorded|p9-11|||Artesian water.||||||
15540|Precipice Sandstone|44032|14|Not recorded|p462,464|||||||||
15540|Precipice Sandstone|44034|6|Mentioned|Tb.1|||||||||
15540|Precipice Sandstone|44084|14|Not recorded|p20,22,24,26,32||Early Jurassic|||||||
15540|Precipice Sandstone|44091|14|Not recorded|p54||Jurassic|||||||
15540|Precipice Sandstone|44095|2|Defined|p284-5|||||||||
15540|Precipice Sandstone|44116|14|Not recorded|p24,28,33|||||||||
15540|Precipice Sandstone|44118|14|Not recorded|Map Legend||Jurassic|||||||
15540|Precipice Sandstone|44124|14|Not recorded|p2,5,10,15-16|||||||||
15540|Precipice Sandstone|44163|4|Described|p1,2,10-14,19,20,||Triassic|Pl.1.||||||
15540|Precipice Sandstone|44169|2|Defined|Tb.1,p6,8,9,12,map|||||||||
15540|Precipice Sandstone|44170|2|Defined|p1,17,20-23,25,27,31||Early Jurassic|p32,35,40,Tb.1,map||||||
15540|Precipice Sandstone|44172|14|Not recorded|p1326,1330,1339||Jurassic|Springsure area.||||||
15540|Precipice Sandstone|44174|14|Not recorded|p345,347,348||Early Jurassic|||||||
15540|Precipice Sandstone|44207|14|Not recorded|p115|||||||||
15540|Precipice Sandstone|44304|14|Not recorded|p1|||||||||
15540|Precipice Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
15540|Precipice Sandstone|44360|14|Not recorded|p36||Early Jurassic|||||||
15540|Precipice Sandstone|44379|4|Described|p1,2,20,21,24,map.||Early Jurassic|||||||
15540|Precipice Sandstone|44381|14|Not recorded|p7|||||||||
15540|Precipice Sandstone|44390|14|Not recorded|p6,8,9,12-16,Tb.1||Early Jurassic|||||||
15540|Precipice Sandstone|44391|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|44414|14|Not recorded|p114||Jurassic|||||||
15540|Precipice Sandstone|44415|14|Not recorded|Fig.2,p23,24|||||||||
15540|Precipice Sandstone|44420|14|Not recorded|p1,3,9,11,18,21,22,|||p25,28,Fig.14||||||
15540|Precipice Sandstone|44421|14|Not recorded|p5,8-11,14,15,17-20||Jurassic|||||||
15540|Precipice Sandstone|44422|14|Not recorded|p148,149,153,154||Early Jurassic|||||||
15540|Precipice Sandstone|44426|14|Not recorded|p12||Jurassic|||||||
15540|Precipice Sandstone|44524|14|Not recorded|p17|||||||||
15540|Precipice Sandstone|44566|14|Not recorded|p13,15-17,Pls.2,3|||||||||
15540|Precipice Sandstone|44567|14|Not recorded|p11,13,14,Pls.1,2|||||||||
15540|Precipice Sandstone|44568|14|Not recorded|p1,4,7,Pls.2,3|||||||||
15540|Precipice Sandstone|44573|14|Not recorded|p97|||||||||
15540|Precipice Sandstone|44585|14|Not recorded|p45-Fig.2|||||||||
15540|Precipice Sandstone|44610|14|Not recorded|49,Tb.1|||||||||
15540|Precipice Sandstone|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
15540|Precipice Sandstone|44627|14|Not recorded|p139,141-144|Jurassic|Triassic|||||||
15540|Precipice Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
15540|Precipice Sandstone|44640|14|Not recorded|p30|||||||||
15540|Precipice Sandstone|44652|14|Not recorded|p73(Tb.),74|||||||||
15540|Precipice Sandstone|44673|14|Not recorded|p25|||||||||
15540|Precipice Sandstone|44742|14|Not recorded|p91|||Lower part correlated with Razorback Beds in Liassic on palynological evidence.||||||
15540|Precipice Sandstone|44787|14|Not recorded|p122-126,128-129,Tb||Jurassic|Basal Jurassic||||||
15540|Precipice Sandstone|44805|14|Not recorded|p388|||||||||
15540|Precipice Sandstone|44840|14|Not recorded|p32,40|||Roma Shelf.||||||
15540|Precipice Sandstone|44844|14|Not recorded|p154||Early Jurassic|Moonie.||||||
15540|Precipice Sandstone|44852|14|Not recorded|p78|Jurassic|Triassic|||||||
15540|Precipice Sandstone|45071|3|Fully described|Table 15|||||||||
15540|Precipice Sandstone|45073|6|Mentioned|p58|||Geological history||||||
15540|Precipice Sandstone|45095|6|Mentioned|p62|||||||||
15540|Precipice Sandstone|45110|2|Defined|p85|Early Jurassic|Early Jurassic|See also Fig.5 and P24.||||||
15540|Precipice Sandstone|45168|6|Mentioned|p6|||||||||
15540|Precipice Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
15540|Precipice Sandstone|46984|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|46989|5|Briefly described|Table 1|||||||||
15540|Precipice Sandstone|47404|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47414|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47448|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47624|14|Not recorded|?|||||||||
15540|Precipice Sandstone|48600|14|Not recorded|p15|||||||||
15540|Precipice Sandstone|48606|14|Not recorded|p5,6,11,13,14,19-22|||(H/55-8 ; G/55-12). Pl.2||||||
15540|Precipice Sandstone|48619|14|Not recorded|?|||||||||
15540|Precipice Sandstone|48898|5|Briefly described|p2|||L.Jurassic. See also PP60,61,83||||||
15540|Precipice Sandstone|48900|4|Described|p50|||||||||
15540|Precipice Sandstone|48919|2|Defined|p36|Early Jurassic|Early Jurassic|See also p37-45.||||||14-FEB-07
15540|Precipice Sandstone|48920|3|Fully described|p36|||Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
15540|Precipice Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
15540|Precipice Sandstone|50190|5|Briefly described|p17, 85|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
15540|Precipice Sandstone|50197|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50209|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50215|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick-bedded, cross-bedded, fine- to coarse-grained pebbly quartzose sandstone and minor lithic sublabile sandstone, siltstone and mudstone.||||||18-JUN-09
15540|Precipice Sandstone|50301|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50317|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick bedded, cross-bedded fine to coarse-grained, pebbly quartzose sandstone, and minor lithic sublabile sandstone, sitlstone and mudstone.||||||09-JUN-04
15540|Precipice Sandstone|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Surat Basin||||||
15540|Precipice Sandstone|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick/cross bedded pebbly quartzose sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|60114|6|Mentioned|p16|||Oil-bearing deposits.  Geological Province:  Cooper - Eromanga Basins.||||||
15540|Precipice Sandstone|60281|5|Briefly described|p27||Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
15540|Precipice Sandstone|60282|5|Briefly described|p11, p30|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
15540|Precipice Sandstone|60557|5|Briefly described|p19 Fig. 5b, p28|Early Jurassic|early Jurassic|Fluviatile sandstones.||||||09-JUN-05
15540|Precipice Sandstone|60995|6|Mentioned|p62|||Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|60996|6|Mentioned|p87|||Geological Province: Surat Basin. Equivalent to the Ripley Road Sandstone in the Clarence-Moreton Basin.||||||
15540|Precipice Sandstone|60998|5|Briefly described|p145|||Overlain by Evergreen Formation.||||||
15540|Precipice Sandstone|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Ripley Road Sandstone and Helidon Sandstone.||||||
15540|Precipice Sandstone|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick-bedded, cross-bedded, fine to coarse-grained, pebbly quartzose sandstone and minor lithic sublabile sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|61310|6|Mentioned|p21, p22|||Geological Province: Surat Basin. Correlated with the "Middle Bundamba Unit".||||||
15540|Precipice Sandstone|61377|5|Briefly described|p151|Early Jurassic|Early Jurassic|Braided stream sandstones. Conformably overlain by Evergreen Formation. Geological Province: Surat Basin. See also p139, p149 Fig. SU8.||||||07-FEB-11
15540|Precipice Sandstone|61611|5|Briefly described|p264, p266, p265 Fig. 3|Early Jurassic|Late Triassic|Lateral equivalent of Myrtle Creek Sandstone. Geological Province: Surat Basin.||||||15-JUL-13
15540|Precipice Sandstone|61832|5|Briefly described|p187, p190|Jurassic|Early Jurassic|On the MUNDUBERRA sheet.  Overlain by Evergreen Formation. Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|62357|5|Briefly described|p535|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Jurassic|Early Jurassic|Surat Basin.||||Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|63979|6|Mentioned|p33, Fig. 44|Toarcian|Pleinsbachian|Overlain by Evergreen Formation. Geological province: Surat Basin. Time-equivalent of Poolowanna Formation.||||||07-FEB-11
15540|Precipice Sandstone|64197|6|Mentioned|p630 Fig.7|Early Jurassic|Early Jurassic|||||Underlies Evergreen Formation.||
15540|Precipice Sandstone|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Overlies Cynthia beds; below Evergreen Formation. Poorly sorted, thick bedded, x-bedded, fine- to v. coarse-gr., pebbly quartzose sst; minor laminated siltstone (upper part), carbonaceous shale, lithic sublabile sandstone, granule conglomerate.||||||19-AUG-08
15540|Precipice Sandstone|64665|5|Briefly described|p53 Fig.2, p57, p60, p61.|Early Jurassic|Early Jurassic|Eromanga and Surat Basins. Lateral equivalent of uppermost Poolowanna Formation. With the Evergreen Formation, forms the first of six cyclothems in the Surat Basin.||||Disconformably overlies Callide Coal Measures. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|64856|3|Fully described|p46 Fig.4, p61-62, p69, p75-76, p78-83|Sinemurian|Late Hettangian|Whitehouse (1952), for lowermost formation of the Bundamba Series. Type area described. Surat Basin. Unconformably overlies Bowen Basin units. Is overlain by Evergreen Formation. Up to 106m thick. Age from palynoflora (units APJ1, 21, 22). Grades laterally into Helidon Sandstone. Cross bedded pebbly quartzose sandstone, minor lithic sandstone, siltstone, argillite.|| ||||29-NOV-17
15540|Precipice Sandstone|64857|4|Described|p130-132, p113 Fig.3|Early Jurassic|Late Triassic|Overlies Bowen Basin sequence. Surat Basin. Mainly fine to coarse-grained pebbly quartzose sandstone. Braided stream deposition.||||||17-NOV-15
15540|Precipice Sandstone|64858|5|Briefly described|p181 Tb.1, p183, 187-188|||Basal Surat Basin unit in the central and northeastern part of the basin.||||||30-NOV-09
15540|Precipice Sandstone|64859|6|Mentioned|p194|Early Jurassic|Early Jurassic|Hydrocarbon reservoir, Surat Basin.||||||
15540|Precipice Sandstone|65003|5|Briefly described|p8, p31||Early Jurassic|Of Surat Basin.||||Overlain by the Evergreen Formation.||
15540|Precipice Sandstone|65096|6|Mentioned|p373|||Surat Basin. Compared with the Jurassic sandstones east of the Kumbarilla Ridge [accidently capitalised as Jurassic Sandstone] and the Ripley Road Sandstone of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||||
15540|Precipice Sandstone|65112|6|Mentioned|Fig 11 p324|Early Jurassic|Early Jurassic|Unit in the Surat Basin. Underlies the Evergreen Sandstone.||||||22-MAR-12
15540|Precipice Sandstone|65113|5|Briefly described|p349, Fig 4 P340|Early Jurassic|Early Jurassic|Underlies the Evergreen Formation.||||||
15540|Precipice Sandstone|65114|5|Briefly described|p385 Fig.3, p383|Early Jurassic||Basal section of Supersequence J; basal Surat Basin||||||
15540|Precipice Sandstone|65116|5|Briefly described|p454, Fig 2 p437|Early Jurassic|Early Jurassic|Underlies the Evergreen Formation, Surat Basin. Quartzose sandstone.||||||
15540|Precipice Sandstone|65117|4|Described|p461, 6, 7, 9, 473, 4, Fig 4 p 465|Sinemurian|Sinemurian|Surat Basin, is overlain by Evergreen Formation with gradational contact. Unconformable over Tamworth Belt or Bowen Basin successions. Potential reservoir. Up to 150m thick in north. Average 60-80m thick. Included in Supersequence J||||||
15540|Precipice Sandstone|65118|6|Mentioned|p483, p493|Early Jurassic|Early Jurassic|Of Surat Basin||||||
15540|Precipice Sandstone|65119|5|Briefly described|p513, Fig 2, Table 1, Fig 4-5,7-13,15-17|Early Jurassic|Early Jurassic|Surat Basin. Quartzose sandstone, pebbly sandstone. Alluvial deposition up to 150m thick. Age: 198-205 Ma. Fission Track age: 98-120 Ma. Present in The Cockatoo Creek Well.||||||
15540|Precipice Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlain by Evergreen Formation.||||||08-MAR-12
15540|Precipice Sandstone|65388|4|Described|p208-211; p 210 Fig. 74, p203, p19|Pliensbachian|Sinemurian|Surat and Mulgilie Basins. Originally lowermost formation of the "Bundamba Series" of Whitehouse (1953). 30m to almost 150m thick. Unconformably overlies Muncon Volcanics, Winterbourne Volcanics, Cynthia beds, Torsdale Volcanics or Devonian to Permian rocks. Overlain by Evergreen Formation. Grades laterally into Helidon Sandstone of Moreton Basin in SE. Age on palynology: APJ1, APJ21 (Sinemurian-early Pliensbachian). White, thick-bedded, cross-stratified, fine to coarse-grained, pebbly quartzose sandstone with only minor lithic sublabile sandstone, siltstone and argillite.||||||
15540|Precipice Sandstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Moolayember Formation. Is overlain by Evergreen Formation.|Medium grained sandstone, non-marine.|
15540|Precipice Sandstone|66915|5|Briefly described|p6 Fig.3, p12|Early Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
15540|Precipice Sandstone|67133|5|Briefly described|p1-3, p5, p8, p10, p19-21|Jurassic|Jurassic|Surat Basin. A carbon geostorage target reservoir, sealed by Evergreen Formation. Large braided-stream deposits. 44 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (40-98%) and kaolinite (2-47%) is the dominant clay mineral.||||Overlies Peawaddy Formation. Is overlain conformably by Evergreen Formation.|A lower unit of predominantly coarse-grained quartzose sandstone, with thin to thick beds and a white clay matrix, is overlain by an upper fine- to medium-grained, thinly-bedded and sublabile unit.|
15540|Precipice Sandstone|67402|4|Described|p18 fig WSD2, p43 tbl HPB1|Pliensbachian|Sinemurian|Bowen and Surat Basins. Major aquifer that is also a highly prospective reservoir for the storage of carbon dioxide. Maximum thickness of 150m. Estimated storage potential of 1289 megatonnes of carbon dioxide. Deposited in a braided river system. See also p48, p56, p72, p146 fig SRT3, p147, p147 fig SRT5, p148, p151, p154, p155 fig SRT17, p156, p158, p162, p236, p239, p242, p243, p252, p253, p306.||||Overlies the Moolayember Formation and the Callide Coal Measures. Overlain by the Evergreen Formation or the Biloela Formation. Equivalent to the Myrtle Creek Sandstone.|Quartzose sandstone with a clay matrix that is overlain by fine-grained sandstone and siltstone.|
15540|Precipice Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Evergreen Formation. Underlain by Molyamber Formation or Wandoan Sandstone.||
15540|Precipice Sandstone|67788|6|Mentioned|p24|Early Jurassic|Early Jurassic|Carnarvon Gorge, QLD. Photograph illustrating broad alluvial plains formed by braided rivers.||||||
15540|Precipice Sandstone|68003|5|Briefly described|p57 Fig.3-n, p58 Fig.3-o.|Early Jurassic|Early Jurassic|Bowen Basin.||||Unconformably overlies Moolayember, Wandoan, and locally Napperby Formations. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|68004|5|Briefly described|pp172-174.|Early Jurassic|Early Jurassic|Petroleum-producing. Excellent reservoir; exploration targetting limited to very northern part of the Basin in NSW. Sealed in Queensland by Evergreen Formation, but in NSW that unit is sandy.||||||
15540|Precipice Sandstone|68008|3|Fully described|p3, p192-194, p203, p208-210, p219-223|Early Jurassic|Early Jurassic|See also p225-238, p246, p251-252, p254, p261-265, p292, p359, p361, p363, p372, p492-493, p621. Whitehouse (1953, 1955). Applied to basal Jurassic sedimentary rocks on the Monto 250k sheet by Dear (1968) and Dear et al. (1971). Includes the Razorback beds of Staines (1953) and Kirkegaard et al. (1970). Occurs mainly in four areas (listed and mapped). Almost always occurs as a ridge-capping, cliff-forming unit. N-flowing braided stream deposits. 45-100m thick. Age from spore assemblage. 6km E of Westwood, vertical columnar jointing occurs; the result of heating by (now eroded) Dalma Basalt. Has long been quarried for building stone; gold was mined at Mount Victoria. Geophysics modelling. Unconformably overlies Muncon, Winterbourne Volcanics, Annie Creek beds, Bushley Dacite, Callide Coal Measures, Bundaleer Tonalite, Quarry Gabbro, Moonmera Porphyritic Granodiorite, possibly Native Cat Andesite, and Flaggy Quartz Monzodiorite.||||Is overlain conformably by Evergreen Formation and unconformably by Dalma Basalt, Biloela Formation and Stanwell Formation. Equivalent to Helidon Sandstone. See Comments.|Extensive but thin sand sheet. Cream, white to buff quartzose sandstone, pebbly quartzose sandstone, and some siltstone; some conglomerate beds. Local well-developed columnar jointing.|21-SEP-18
15540|Precipice Sandstone|68117|6|Mentioned|p346|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|68135|5|Briefly described|p52 fig 2b, p59, p63 fig 6,  p64|Pleinsbachian|Sinemurian|Surat Basin (QLD). Age confirmed by dinosaur footprints. Plant macrofossils and vertebrate body parts and footprints found throughout.||||Overlain by Evergreen Formation|Sandstone.|14-SEP-17
15540|Precipice Sandstone|68139|6|Mentioned|p23|Early Jurassic|Early Jurassic|Surat Basin.||||Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
15540|Precipice Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Evergreen Formation and Hutton Sandstone, are all mapped under the symbol, Jb.||||||
15540|Precipice Sandstone|68576|5|Briefly described|Q_4: p1, p3-5, p12-15, p21-22, p24|Early Jurassic|Early Jurassic|The basal unit in the Surat Basin. The unconformity represents a 40 m.y. hiatus and separates the Bowen Basin from the Surat Basin. A major aquifer. Forms the majority of cliff faces in Carnarvon Gorge. Displays braided fluvial sedimentary structures.||||Unconformably overlies Taroom and Eddystone beds, and Moolayember Formation. Is overlain conformably by Evergreen Formation.|Fine- to coarse-grained, pebbly quartzose sandstone with minor lithic sub-labile sandstone, siltstone and argillite.|
15540|Precipice Sandstone|68679|5|Briefly described|p312-313, p338, p398, p443|Jurassic|Jurassic|Northern New England Orogen. Covers much of the Callide Basin fill. A scarp-forming unit. Previously (Dear et al. , 1971) included in the Callide Coal Measures, but excluded on palynological grounds by de Jersey (1974).||||Disconformably or unconformably overlies Callide Coal Measures. Overlies Winterbourne Volcanics.||
15540|Precipice Sandstone|69457|5|Briefly described|p41:2-3|||NE Eromanga Basin and Surat Basin.|||Is overlain by Evergreen Formation.|Lateral equivalent of (part) Poolowanna Formation.||12-JUL-16
15540|Precipice Sandstone|69582|6|Mentioned|p35-p36, p38|Lower Jurassic|Lower Jurassic|Surat Basin.||||Overlain by the Evergreen Formation.||
15540|Precipice Sandstone|69594|5|Briefly described|p519, p524, p533-535, p539, p543-545|Pliensbachian|Sinemurian|See also p551, p560, p563, p572. Whitehouse (1952, 1955) identified a lower coarse subunit and an upper finer unit; the lower subunit is regarded as the formation (Green et al., 1997). Eromanga, northern Surat Basins. ~45m thick, thinning rapidly to the NW (also said to be up to 106m thick). Braided stream deposits. In the Mount Morgan and Stanwell areas, the Razorback beds are recognised as outliers of the Precipice Sandstone. Has a diachronous base younging to the W. The main Surat Basin reservoir for oil condensate, gas and LPG. Groundwater aquifer. RELATED UNITS (continued): Passes laterally into Poolowanna Formation. Merges with Ripley Road Sandstone in the Surat Basin. Upper part correlated with Gatton Sandstone.||||Unconformably overlies Eddystone beds, Moolayember Formation and Chong beds. Is overlain by Stanwell Formation, Dalma Basalt and conformably by Evergreen Formation. See COMMENTS for more.|Thick-bedded, coarse, quartzose sandstone.|
15540|Precipice Sandstone|69633|4|Described|p1-15, p20, Appendix 6.|Early Jurassic|Early Jurassic|Surat Basin. Hydrocarbon reservoir, sealed by Evergreen Formation. Has a widespread unconformity at its base. Fresh-water, fluvial braided-channel sediments succeeded by fluvio-lacustrine deposits. GSQ Chinchilla 4 and Roma 8 core logs detailed (Appendix 4 & 5). The authors argue that at least part of the lowest c.58m of the Evergreen Formation, ie below the Boxvale Sandstone Member, should be assigned to this unit. Palynology detailed. Data from sections from well completion reports are included in Appendix 1 and 2.||||Unconformably overlies Chong beds and Eddystone beds. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|69681|5|Briefly described|p74-87|Early Jurassic|Early Jurassic|Primary target for oil and gas exploration: has good porosity and high permeability, although permeability decreases by an order of magnitude below ~1500m. Yields oil in the Moonie field. Most of the core samples used for this study are from this unit and the Evergreen Formation. Potential for CO2 geostorage, sealed by Evergreen Formation, discussed.||||Is overlain by Evergreen Formation.|Sandstone; shale and siltstone common in upper part of this unit.|
15540|Precipice Sandstone|69682|4|Described|p91-110|Early Jurassic|Early Jurassic|Basal Surat Basin. Potential CO2 reservoir. 70m thick. Mineralogy discussed in detail. Conclusion is that it is suitable for residual pore-space, hydrodynamic and dissolution sequestration of CO2.||||Is conformably overlain by Evergreen Formation.|Laterally extensive, predominantly quartzose, fine- to very coarse-grained sandstone with pebbly horizons and minor siltstone.|
15540|Precipice Sandstone|69790|6|Mentioned|p1062|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|70374|6|Mentioned|p809 figure 1|Pliensbachian|Sinemurian|||||Is overlain by Evergreen Formation.||28-SEP-16
15540|Precipice Sandstone|70628|6|Mentioned|p952,964|Sinemurian|Sinemurian|Along with Evergreen Formation, forms part of the J-sequence (Hoffman et al 2009) of the Surat Basin.||||Underlies Evergreen Formation.|Sandstone.
|
15540|Precipice Sandstone|70821|5|Briefly described|p79-80|||Eromanga, Surat Basins. A deep, high-quality aquifer in the Great Artesian Basin.||||Unconformably overlies Moolayember Formation. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|71282|6|Mentioned|p457 Fig.1, p460|||The lithology is omitted in Fig.1. Appears as Evergreen & Precipice Formation on p460.||||||
15540|Precipice Sandstone|71805|4|Described|p75-p78, p80-p89|Toarcian|Sinemurian|Surat Basin. The term Precipice Sandstone was first used by Whitehouse (1952) who defined the type section as "Sandstone cliffs in the gorge of precipice Creek, a tributary of the Dawson River" located on the Taroom Sheet of Mollan et al. 1972. Further nomenclature details are provided by Exon (1976). This unit youngs to the west. This unit is a regional aquifer and ranges from less than 10m to nearly 150m in thickness. Informally referred to as upper and lower components. An upper and lower facies are described. Wireline logs exist for the core and for this unit.||||Overlies the Moolayember Formation. Conformably overlain by the Evergreen Formation.  Placement of boundary with Evergreen Formation discussed.|Quartzose sandstones, siltstone and mudstones with rare thin coals.|16-MAY-19
15540|Precipice Sandstone|71806|4|Described|p483-p488, p500|Lower Jurassic|Lower Jurassic|Surat Basin. Traditionally interpreted as a braided fluvial deposit; however, this study also found evidence of tidal to marine influence. This unit is an important aquifer and petroleum reservoir. Unconformably to disconformably overlies Permo-Triassic strata. Varies from over 150m in the axis of the basin to less than 20m on the eastern and western margins. Exposed in Boolimba Bluff. Lithology is derived from the 'informal type section' at Boolimba Bluff. Facies are described in detail.||||Overlain by the Evergreen Formation.|Very coarse- to medium-grained quartz arenite, fine- to very fine-grained quartz arenite with kaolinite clay matrix, granule to medium-pebble conglomerate and siltstone to mudstone beds.|
15540|Precipice Sandstone|72297|5|Briefly described|p697, p724, p726, p739, p744-746, p748|Early Jurassic|Early Jurassic|At Grafton Range, NE of Roma, contains sodium bicarbonate in high-salinity brines 800-1000m below ground surface. The bicarbonate originates from the underlying Aldebaran Sandstone. An excellent regional reservoir; produced the first commercial oil discovery in Australia (UOD Moonie, 210km SE of Roma) in 1961. Sealed by Evergreen Formation.|||Razorback beds.|Disconformably overlies the Callide Coal Measures.|Fluvial sheet sandstone.|
15540|Precipice Sandstone|72298|5|Briefly described|p790, p796, p801-802|Jurassic|Jurassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores. An aquifer which locally exhibits double porosity (primary porosity/permeability, and secondary porosity resulting from faulting and/or dissolution of silica). A source of groundwater in the Monto area. Crops out in the Great Dividing Range but has no specific discharge point.||||Unconformably overlies Moolayember and Wandoan FZs. Is overlain by Evergreen FZ.||
15540|Precipice Sandstone|72921|4|Described|p8-10, p15 Fig.2, p16-17, p21 Fig.7.|Early Jurassic|Early Jurassic|Site of demonstration effort aiming to inject 180,000 tons of CO2 as part of Surat Carbon Capture and Storage (CCS) project. Shown as located in the Surat Basin in Queensland. Sediments demonstrate a marine influence. See also p23 Fig.9, p24-25, p27-28, p48-p52, p54, p55, p77 App.1, p82.||||Conformably underlies Evergreen Formation|Includes sandstone and conglomerate and fossils.|
15540|Precipice Sandstone|73113|5|Briefly described|p. 2-3, 22-24, 29-31, 35-37, 41, 46...|||Surat Basin. Regional aquifer. Treated water is re-injected into this unit (since 2015). Relatively high incidences of fracturing in the unit. More locations: p. 60, 66-67, 69, 79-80, 92, 98, 116-117, 119, 123, 126-127, 130, 148-149, 152-153, 159-160, 162, 164, 168-173, 177, 179, 182-183, 191-193, 199.||||Unconformably underlain by Rewan Group, Bandanna Formation, Cattle Creek Formation, and Moolayember Formation. Overlain by Evergreen Formation.||
15540|Precipice Sandstone|73147|5|Briefly described|p127|Early Jurassic|Early Jurassic|Surat Basin.|||||Marine influenced.|
15540|Precipice Sandstone|73393|6|Mentioned|p20-21|Toarcian|Pliensbachian|Surat and Eromanga Basins.||||||
15540|Precipice Sandstone|73450|6|Mentioned|p51|||||||Underlain by Bushley Dacite.||
15540|Precipice Sandstone|73570|6|Mentioned|p914, p915 Fig.4, p916, p917 Fig.5|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|73600|4|Described|p189-192, p195-199, p201-205|Pliensbachian|Sinemurian|Surat Basin. Economically important due to its aquifer capacity and prospectivity for CO2 sequestration. Variable thickness with a maximum of ca 175 m. Gradational upper boundary. Comprises two main parts, a 'lower' and 'upper'. Grade from quartzose to more labile and mineralogically heterogeneous up-section. Interpreted to represent braided through to meandering fluvial settings, fluvial-lacustrine systems, and marine depositional settings. Palynology was previously used for biostratigraphic age constraint. Contains no known tuff horizons. Various detrital zircon maximum depositional ages are presented. Detrital zircon age spectra demonstrate complex sediment sourcing dominated by the Thomson Orogen. Absent on the Kumbarilla and Nebine ridges. Relatively uniform provenance and sediment characteristics across the study area.||||Conformably overlain by Evergreen Formation. Underlain by Eddystone Beds. Unconformably underlain by the Moolayember Formation.|Coarse-grained, thick-bedded sandstone capped by an overall fining-upward, fine- to medium-grained sandstone.|
15615|Proserpine Volcanics|23277|6|Mentioned|p59|||(Clarke et al., 1971).||||||
15615|Proserpine Volcanics|23911|6|Mentioned|p87|||Geological Province: Whitsunday Volcanic Province.||||||
15615|Proserpine Volcanics|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15615|Proserpine Volcanics|32553|4|Described|p38|||||||||
15615|Proserpine Volcanics|32554|6|Mentioned|p8|||||||||
15615|Proserpine Volcanics|32555|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15615|Proserpine Volcanics|34408|6|Mentioned|p185|||On table||||||
15615|Proserpine Volcanics|35460|6|Mentioned|p152|||||||||
15615|Proserpine Volcanics|35872|6|Mentioned|p457|||See also Table 1.||||||
15615|Proserpine Volcanics|36472|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
15615|Proserpine Volcanics|36906|6|Mentioned|p25|||||||||
15615|Proserpine Volcanics|36961|6|Mentioned|Table 1|||||||||
15615|Proserpine Volcanics|37675|6|Mentioned|p2|||||||||
15615|Proserpine Volcanics|39445|5|Briefly described|Table 11|||||||||
15615|Proserpine Volcanics|40245|6|Mentioned|p189|||||||||
15615|Proserpine Volcanics|40574|6|Mentioned|p5|||||||||
15615|Proserpine Volcanics|42281|5|Briefly described|p71|||||||||
15615|Proserpine Volcanics|45151|5|Briefly described|Table 12|||||||||
15615|Proserpine Volcanics|48921|2|Defined|p45|Early Cretaceous|Early Cretaceous|See also Table 2||||||
15615|Proserpine Volcanics|64570|5|Briefly described|p855, p858|Early Cretaceous|Early Cretaceous|Age: 113 (111)+/-5Ma. Mostly rhyolitic lava flows.||||||27-FEB-09
15615|Proserpine Volcanics|65706|4|Described|p12, p18 Tb.1|Early Cretaceous|Early Cretaceous|Probably terrestrial equivalents of the Whitsunday Volcanics.||||Unconformable on Edgecumbe beds and Airlie Volcanics.|Rhyolite, andesite and minor volcaniclastics.|
15615|Proserpine Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Whitsunday Province. This unit, as well as the Whitsunday Volcanics and unnamed volcanic units, are all mapped under the symbol, Kv.||||||
15615|Proserpine Volcanics|68679|6|Mentioned|p347, p364|Cretaceous|Cretaceous|Northern New England Orogen.||||||
15615|Proserpine Volcanics|68901|6|Mentioned|p2 Fig. i|Cretaceous|Cretaceous|||||||27-SEP-18
15615|Proserpine Volcanics|69594|5|Briefly described|p552-554, p557-558|Early Cretaceous|Early Cretaceous|Clarke et al. (1971). Whitsunday Volcanic Province. >1km thick sequence. Occurs along the coast. Coeval with Whitsunday Volcanics. Lithologies and vulcanism very detailed.||||Contiguous with Whitsunday Volcanics.|Silicic to intermediate extracaldera pyroclastic rocks and minor lavas; mafic lavas (basalt and basaltic andesite) are significant with abundant mafic dykes; ignimbrite sheets lack coarse, lithic-lag breccias. Extensive (>300 km2) fluidal rhyolite.|
15615|Proserpine Volcanics|69952|6|Mentioned|p85|Cretaceous|Cretaceous|||||||
15641|Puckley Granite|12575|6|Mentioned|p781, p784 Table 1.|Permian|Permian|I-type granite. Northeastern Hodgkinson Province. Apatite fission track analyses are detailed.|276-264 Ma.|Unit in Yates Supersuite.||||
15641|Puckley Granite|23423|5|Briefly described|p252 + p284||Early Permian|Yates Supersuite||||||
15641|Puckley Granite|23426|5|Briefly described|p402.|||||||||
15641|Puckley Granite|23511|5|Briefly described|Map Legend||Early Permian|Age: 276 +/- 3Ma.||||||
15641|Puckley Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
15641|Puckley Granite|31435|6|Mentioned|p17|||||||||
15641|Puckley Granite|39445|5|Briefly described|Table 12|||||||||
15641|Puckley Granite|42369|6|Mentioned|p55|||||||||
15641|Puckley Granite|42490|5|Briefly described|p14|||||||||
15641|Puckley Granite|43070|2|Defined|p23|Early Permian||Radiometric date of 275 Ma. Of Yates Supersuite||||||23-APR-09
15641|Puckley Granite|43098|5|Briefly described|p39|||Rb-Sr rock-biotite age of 276+/-3Ma.||||||
15641|Puckley Granite|43111|6|Mentioned|p1|||||||||
15641|Puckley Granite|43896|14|Not recorded|Map Legend||Permian|||||||
15641|Puckley Granite|43979|14|Not recorded|p67||Permian|||||||
15641|Puckley Granite|44258|14|Not recorded|p5,11,16,35||Early Permian|||||||
15641|Puckley Granite|44267|14|Not recorded|Map Legend||Permian|||||||
15641|Puckley Granite|44292|2|Defined|Tb.1,p8,map||Permian|Correlated with Mareeba Granite. Intrudes Hodgkinson Formation.||||||
15641|Puckley Granite|44293|14|Not recorded|Map Legend||Permian|||||||
15641|Puckley Granite|44294|2|Defined|Tb.2,p11,14,map|||||||||
15641|Puckley Granite|45025|4|Described|p78-79||Permian|||||||
15641|Puckley Granite|45113|3|Fully described|p22|||Emphasis on petrography.||||||
15641|Puckley Granite|48894|6|Mentioned|p58|||Age||||||
15641|Puckley Granite|60425|4|Described|p91, p272-3 Appdx. 1|Early Permian|Early Permian|Of Puckley Suite (Yates Supersuite). I-type. Also written as Puckley granite (p179). Age: 276+/-3Ma (Rb-Sr). Med-gr., moderately porphyritic (hornblende?-) biotite granite; minor hornblende-biotite granodiorite; accessory minerals - for details see p273.||||||07-FEB-11
15641|Puckley Granite|69593|5|Briefly described|p480, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|276 +/- 3 Ma.|Yates Supersuite.|||I-type.|
15641|Puckley Granite|72983|6|Mentioned|p3, p35, p38|Roadian|Kungurian|Similar age and lithology to the Hope Vale Granite.|276 +/- 3 Ma Rb-Sr|Yates Supersuite||||
15641|Puckley Granite|73083|6|Mentioned|p61|Permian|Permian|||||||
15643|Puddler Granodiorite|42633|6|Mentioned|Table 1 p8|||Typo for Puddler Creek Formation, or new name?||||||11-MAY-18
15655|Pumpkin Hut Mudstone|24076|5|Briefly described|p397 Fig. 2|Middle Devonian|Middle Devonian|Max. thickness: 1000m. Geological Province: Yarrol Basin.||||||14-APR-08
15655|Pumpkin Hut Mudstone|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
15655|Pumpkin Hut Mudstone|32388|6|Mentioned|Fig.1|||||||||
15655|Pumpkin Hut Mudstone|33774|3|Fully described|p13|||||||||
15655|Pumpkin Hut Mudstone|36333|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Early to Middle Devonian.||||||18-AUG-08
15655|Pumpkin Hut Mudstone|39445|5|Briefly described|Table 5|||||||||
15655|Pumpkin Hut Mudstone|39632|6|Mentioned|p223|||||||||
15655|Pumpkin Hut Mudstone|42031|5|Briefly described|Fig.3 P759|||||||||
15655|Pumpkin Hut Mudstone|42868|5|Briefly described|p28|||||||||
15655|Pumpkin Hut Mudstone|43008|5|Briefly described|map legend|||||||||
15655|Pumpkin Hut Mudstone|61761|6|Mentioned|p4|||Consists of lithic and feldspathic mudstone.||||||07-FEB-11
15655|Pumpkin Hut Mudstone|64398|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Arenite, siltstone, mudstone.||||||
15655|Pumpkin Hut Mudstone|68553|6|Mentioned|Map legend; schematic diagram.|Devonian|Devonian|Calliope Province. This unit, as well as the Capella Creek Group, the Erebus, Marble Waterhole, Craigilee, Calliope, Munbooree and Dunollie beds, are all mapped under the symbol, Dc.||||||
15655|Pumpkin Hut Mudstone|68679|5|Briefly described|p312-313, p317|Middle Devonian|Early Devonian|Driscoll (1960). Philpott Subprovince, northern New England Orogen. Extends in a fault-bounded belt from the N end of the Munbooree beds northwards to include most of the drainage of Philpott Creek straddling the Burnett Highway. Age based on regional stratigraphy and structure.|||||Feldspatholithic sandstone, siltstone and mudstone with minor calcareous sandstone and basic to intermediate volcaniclastics.|
15717|Quamby Conglomerate|22461|5|Briefly described|p468|||||||||
15717|Quamby Conglomerate|22462|4|Described|P6||Calymmian|Age of unit is 1500 Ma||||||
15717|Quamby Conglomerate|23396|6|Mentioned|p426|||||||||
15717|Quamby Conglomerate|23397|6|Mentioned|p464 Fig.3|||||||||
15717|Quamby Conglomerate|23519|5|Briefly described|p105|Proterozoic|Proterozoic|Geological Province: Eastern Fold Belt.||||||
15717|Quamby Conglomerate|29965|6|Mentioned|p402|||||||||
15717|Quamby Conglomerate|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15717|Quamby Conglomerate|30531|6|Mentioned|p20|||Also mention P22.||||||
15717|Quamby Conglomerate|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
15717|Quamby Conglomerate|31829|6|Mentioned|p29|||Upper Proterozoic||||||
15717|Quamby Conglomerate|32660|5|Briefly described|Table 5|||||||||
15717|Quamby Conglomerate|32959|6|Mentioned|Fig.21|||||||||
15717|Quamby Conglomerate|33214|6|Mentioned|Fig.1|||||||||
15717|Quamby Conglomerate|33900|6|Mentioned|p19|||||||||
15717|Quamby Conglomerate|35074|6|Mentioned|Fig.2|||||||||
15717|Quamby Conglomerate|35939|5|Briefly described|p629|||||||||
15717|Quamby Conglomerate|36332|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Upper Proterozoic (Adelaidean).||||||
15717|Quamby Conglomerate|37565|6|Mentioned|p3|||||||||
15717|Quamby Conglomerate|37569|6|Mentioned|p92|||||||||
15717|Quamby Conglomerate|38278|6|Mentioned|Fig.3|||||||||
15717|Quamby Conglomerate|39445|5|Briefly described|Table 3|||Gold produced. See P55||||||
15717|Quamby Conglomerate|39492|6|Mentioned|p31|||||||||
15717|Quamby Conglomerate|39799|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
15717|Quamby Conglomerate|40840|6|Mentioned|Map legend|||||||||
15717|Quamby Conglomerate|42000|6|Mentioned|p53|||||||||
15717|Quamby Conglomerate|42173|6|Mentioned|Fig.1 P172|||||||||
15717|Quamby Conglomerate|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Conglomerate, sandstone.||||||09-FEB-09
15717|Quamby Conglomerate|44270|14|Not recorded|Map Legend||Neoproterozoic|||||||
15717|Quamby Conglomerate|44271|2|Defined|p40,41,53,59,62,Fg.5||Paleoproterozoic|See also Lexicon.||||||07-NOV-08
15717|Quamby Conglomerate|44275|14|Not recorded|Map Legend|||||||||
15717|Quamby Conglomerate|44278|2|Defined|p8,Tb.1,map|||||||||
15717|Quamby Conglomerate|44989|2|Defined|p.123-4|||Tb.IV. On many pages. Overlies Corella Formation. (F54-2).||||||
15717|Quamby Conglomerate|45166|4|Described|p33|||||||||
15717|Quamby Conglomerate|45287|14|Not recorded|p.223,226,229,232|||||||||
15717|Quamby Conglomerate|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
15717|Quamby Conglomerate|49041|5|Briefly described|Table 3|||||||||
15717|Quamby Conglomerate|50100|6|Mentioned|p13 Fig.4|Calymmian|Calymmian|||||||
15717|Quamby Conglomerate|50332|4|Described|p16, p22, p71, p95|Paleoproterozoic|Paleoproterozoic|Age: 1515Ma. Uncomformably underlain by Corella Formation. Max thickness: 300m. Geological Province: Quamby-Malbon Sudprovince, Eastern Fold Belt Province. Consists of conglomerate, arkose, quartz sandstone, and greywacke.||||||07-FEB-11
15717|Quamby Conglomerate|61933|5|Briefly described|p169 Fig.1|||||||||
15717|Quamby Conglomerate|64248|6|Mentioned|p38 Fig.5|||||||||
15717|Quamby Conglomerate|64250|4|Described|p11 fig 3, p10, p18|Mesoproterozoic|Mesoproterozoic|Mary Kathleen Fold Belt, Mount Isa Inlier. 300m thick outcrops are fault-bound. An age between 1580 Ma and 1490 Ma was obtained from EMP U-Th-Pb analysis of monazite grains (Evins et al. 2007).|||||Conglomerate, feldspathic sandstone, hematitic quartz sandstone and lithic sandstone.|
15717|Quamby Conglomerate|65387|4|Described|p1, p3 Tb.1, p42-49, p82-83|Statherian|Statherian|Deposited in small, laterally discontinuous roughly N-S graben systems. Maximum depositional age from detrital zircons; youngest individual analysis is 1688 +/- 88 Ma. This is considerably older than inferred stratigraphic age and previous age determinations, including 1580-1490 Ma (Evins et al., 2007) whose electron probe monazite age may have been of metamorphic or metasomatic origin. Younger zircons were probably derived from Wonga and Burstall Suites granites.|1754 +/- 10 Ma SHRIMP zircon (Carson et al. 2008)|||Overlies Corella Formation.|Clast-supported lithic pebble to cobble conglomerate.|
15717|Quamby Conglomerate|65396|5|Briefly described|p17, p82, p169, p174-175, p183, p185-186|Calymmian|Statherian|See also p202, p217, p241. Age between 1500 Ma - 1640 Ma discussed in detail. Roughly 300m thick. Host to (minor and abandoned) Quamby Gold deposit. Possible correlative of Knapdale Quartzite.|Between c.1640 Ma and c.1500 Ma (U-Th-Pb).|Mount Albert Group.||Unconformably overlies Corella Formation.|Conglomerate, arkose, hematitic quartz sandstone and greywacke.|
15717|Quamby Conglomerate|66913|5|Briefly described|p188|||40 km north of Cloncurry. Age probably represents diagenesis.|~1490 Ma hydrothermal (lowTh) monazites.|||||
15717|Quamby Conglomerate|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Neoproterozoic|Neoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p107-108. Mary Kathleen Domain, Mount Isa Inlier. Also dated at 1486 +/- 19 Ma (?diagenesis).|1581 +/- 5 Ma (40Ar/39Ar mica).||||Polymictic pebble to cobble conglomerate and pebbly, medium to very coarse-grained lithofeldspathic sandstone.|
15717|Quamby Conglomerate|67499|6|Mentioned|p940|Calymmian|Calymmian|Th-U-Pb electron microprobe dating of detrital monzanite allows bracketing of deposition to be determined.|1580-1490 Ma|Of South Nicholson Group?||||
15717|Quamby Conglomerate|68553|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
15717|Quamby Conglomerate|69056|5|Briefly described|p2, p4, p6, p13, p18, p23, p28, p56|Calymmian|Calymmian|See also Reference images sheet, Time-Space plot sheet. Mary Kathleen Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area. Occurs in small grabens. Modelling values listed.|1580 Ma to ?1490 Ma (monazite: Jell, 2013).|||||
15717|Quamby Conglomerate|69591|5|Briefly described|p29, p53-54|Mesoproterozoic|Mesoproterozoic|Mary Kathleen Domain, Eastern Fold Belt. Fluvial sediments; deposited in small grabens along the Pilgrim Fault and Rose Bee Fault. Mesoproterozoic age based on palaeomagnetic data (Idnurm and Wyborn, 1998). Dated between 1580 Ma and 1490 Ma by Th-U-Pb electron microprobe on monazite (Evins et al., 2007): brief comment. Grouped with Neoproterozoic-Paleozoic units on p29. Gentle folding indicates post-Isan Orogeny. MDA by Evins et al. (2007).|~1580 Ma or (?)1490 Ma (maximum depositional age).||||Polymictic pebble to cobble conglomerate and pebbly, medium- to very coarse-grained lithofeldspathic sandstone; unmetamorphosed.|
15717|Quamby Conglomerate|70355|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Polymictic pebble to cobble conglomerate and pebbly, medium- to very coarse-grained, lithofeldspathic sandstone. A sub-unit of medium- to coarse-grained lithofeldspathic sandstone is mapped separately.|
15717|Quamby Conglomerate|70356|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Polymictic pebble to cobble conglomerate and pebbly, medium- to very coarse-grained, lithofeldspathic sandstone. A sub-unit of medium- to coarse-grained lithofeldspathic sandstone is mapped separately.|
15717|Quamby Conglomerate|70532|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Polymictic pebble to cobble conglomerate and pebbly, medium- to very coarse-grained feldspathic sandstone.|
15717|Quamby Conglomerate|70574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes unnamed member of pebbly, medium to coarse grained lithofeldspathic sandstone.|||Includes an unnamed member.||Polymictic pebble to cobble conglomerate and pebbly, medium-very coarse grained lithofeldspathic sandstone.|
15717|Quamby Conglomerate|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1754+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Conglomerate.|
15717|Quamby Conglomerate|72889|6|Mentioned|p6 Fig.i.|||||||||
15717|Quamby Conglomerate|73083|6|Mentioned|p57|Neoproterozoic|Neoproterozoic|||||||
15717|Quamby Conglomerate|73137|6|Mentioned|p6|Mesoproterozoic|Mesoproterozoic|||||||
15717|Quamby Conglomerate|73413|6|Mentioned|p3, App.1|Statherian|Statherian|Mount Isa Inlier, Eastern Fold Belt, Mary Kathleen [Domain]. U-Pb SHRIMP age of 1754 +/- 10 Ma reported by Carson et al. (2008).|1754 +/- 10 Ma|||||
15717|Quamby Conglomerate|73525|5|Briefly described|p4|Calymmian|Statherian|Mary Kathleen and Mitakoodi-Tommy Creek Domains.|1754+/-10 Ma maximum depositional age||||Conglomerate (-coarse sandstone) siliciclastics.|
15717|Quamby Conglomerate|73553|6|Mentioned|p7, p8 Fig.1.2.3|Mesoproterozoic|Mesoproterozoic||1754+/-10 Ma MDA, 1490 Ma (Th-U-Pb monazite)|||||
15764|Quilalar Formation|22438|4|Described|p535, Fig.3 p537|||See also Fig.10a p546. Quartz-carbonate formation.||||||27-NOV-06
15764|Quilalar Formation|22457|5|Briefly described|P31|||||||||
15764|Quilalar Formation|22498|6|Mentioned|Fig2 P235|||||||||
15764|Quilalar Formation|22585|4|Described|P739, Fig1, Fig2|||||||||
15764|Quilalar Formation|22644|5|Briefly described|5 fig 2|||Geological  province: Mt Isa Basin.||||||18-JAN-07
15764|Quilalar Formation|22665|6|Mentioned|P220||Statherian|||||||
15764|Quilalar Formation|23031|5|Briefly described|21|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt. Overlain by Bigie Formation.||||||07-NOV-08
15764|Quilalar Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1780+/-20Ma.||||||27-NOV-06
15764|Quilalar Formation|23393|4|Described|p18, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
15764|Quilalar Formation|23395|6|Mentioned|p383|||||||||
15764|Quilalar Formation|23396|5|Briefly described|p407 Fig.2|||||||||
15764|Quilalar Formation|23399|6|Mentioned|p489|||||||||
15764|Quilalar Formation|23406|5|Briefly described|p601 Fig.3|||||||||
15764|Quilalar Formation|23466|5|Briefly described|p267|||||||||
15764|Quilalar Formation|23518|4|Described|p9 Fig. 3, p11|Proterozoic|Proterozoic|Geological Province: Western Fold Belt.||||||
15764|Quilalar Formation|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Leichhardt Superbasin.||||||02-APR-07
15764|Quilalar Formation|23965|5|Briefly described|p1297|||||||||
15764|Quilalar Formation|24308|5|Briefly described|p991, p987 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15764|Quilalar Formation|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Erroneously included in the Haslingden Group?  Geological Province: Western Fold Belt, Lawn Hill Subprovince and Leichardt River Subprovince (Mount Isa Orogen).||||||07-NOV-08
15764|Quilalar Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|Reserved as Quilalar.||||||27-NOV-06
15764|Quilalar Formation|36548|6|Mentioned|p517|||||||||
15764|Quilalar Formation|36937|6|Mentioned|p229|||||||||
15764|Quilalar Formation|37459|6|Mentioned|p423|||||||||
15764|Quilalar Formation|37462|4|Described|Table4.VII|||||||||
15764|Quilalar Formation|37568|5|Briefly described|p83|||See also p85.||||||27-NOV-06
15764|Quilalar Formation|38232|6|Mentioned|p81|||See also p85.||||||27-NOV-06
15764|Quilalar Formation|38235|6|Mentioned|p113|||||||||
15764|Quilalar Formation|38237|6|Mentioned|p125|||||||||
15764|Quilalar Formation|38276|6|Mentioned|Fig.1|||||||||
15764|Quilalar Formation|38348|6|Mentioned|p7|||||||||
15764|Quilalar Formation|38350|6|Mentioned|p15|||||||||
15764|Quilalar Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|38560|6|Mentioned|p115|||||||||
15764|Quilalar Formation|38835|6|Mentioned|p164|||||||||
15764|Quilalar Formation|38836|6|Mentioned|p165|||||||||
15764|Quilalar Formation|38900|6|Mentioned|p55|||||||||
15764|Quilalar Formation|38919|6|Mentioned|p496|||||||||
15764|Quilalar Formation|39202|6|Mentioned|p242|||||||||
15764|Quilalar Formation|39362|6|Mentioned|p1468|||||||||
15764|Quilalar Formation|39445|5|Briefly described|Table 2|||Probably continuous with Ballara Quartzite. See also p36 and p40.||||||27-NOV-06
15764|Quilalar Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Lochness Formation.||||||15-JUN-06
15764|Quilalar Formation|39622|6|Mentioned|Fig.2|||See also Appendix||||||
15764|Quilalar Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
15764|Quilalar Formation|39925|6|Mentioned|Fig.9|||||||||
15764|Quilalar Formation|39934|6|Mentioned|Fig.3|||||||||
15764|Quilalar Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
15764|Quilalar Formation|40221|3|Fully described|p11|||||||||
15764|Quilalar Formation|40840|6|Mentioned|Map legend|||||||||
15764|Quilalar Formation|40984|6|Mentioned|p389|||||||||
15764|Quilalar Formation|41277|6|Mentioned|Fig.5|||||||||
15764|Quilalar Formation|41307|4|Described|p11|||||||||
15764|Quilalar Formation|41381|6|Mentioned|p328|||||||||
15764|Quilalar Formation|41791|6|Mentioned|p269|||||||||
15764|Quilalar Formation|41978|6|Mentioned|p494|||||||||
15764|Quilalar Formation|41979|6|Mentioned|p522|||||||||
15764|Quilalar Formation|42234|4|Described|p1055|||||||||
15764|Quilalar Formation|42523|5|Briefly described|p372|||||||||
15764|Quilalar Formation|42565|4|Described|Table 1 P5, P2|||||||||
15764|Quilalar Formation|42676|5|Briefly described|Fig.2 P41|||||||||
15764|Quilalar Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale: commonly calcareous.||||||09-FEB-09
15764|Quilalar Formation|42812|6|Mentioned|p65|||||||||
15764|Quilalar Formation|42818|5|Briefly described|p212|||see also Fig.2 p205.||||||27-NOV-06
15764|Quilalar Formation|43608|6|Mentioned|Fig.11,p11|||||||||
15764|Quilalar Formation|43616|6|Mentioned|p4|||||||||
15764|Quilalar Formation|44195|6|Mentioned|p356 Fig.9|||||||||
15764|Quilalar Formation|45161|6|Mentioned|p27|||||||||
15764|Quilalar Formation|45166|4|Described|p17|||||||||
15764|Quilalar Formation|46960|2|Defined|p221|Proterozoic|Proterozoic|||||||
15764|Quilalar Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
15764|Quilalar Formation|46995|5|Briefly described|p268|||||||||
15764|Quilalar Formation|46996|6|Mentioned|p273|||||||||
15764|Quilalar Formation|47083|4|Described|p10-11||Proterozoic|Previously included as part of 'Surprise Creek Beds'.  Equivalent to Corella Formation. Overlain by Bigie Formation, Fiery Creek Volcanics, Surprise Ceek Formation; conformably underlain by Myally Subgroup.||||||27-NOV-06
15764|Quilalar Formation|49041|5|Briefly described|Table 1|||||||||
15764|Quilalar Formation|50100|5|Briefly described|p11, p13 Fig. 4|Statherian|Statherian|Unconformably overlies the Leichhardt Volcanics.  Age: ~1750Ma.  Geological Province: Western Fold Belt Province.||||||27-NOV-06
15764|Quilalar Formation|50332|5|Briefly described|p16, p17, p18|Paleoproterozoic|Paleoproterozoic|Age: 1755-1740Ma. Unconformably overlain by Bigie Formation, in western area conformably unberlain by Myally Subgroup, in other parts is unconformably underlain by Leichhardt Volcanics.||||||07-FEB-11
15764|Quilalar Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Conformably overlies Myally Subgroup. Overlain by Bigie Formation at an angular unconformity.||||||19-DEC-07
15764|Quilalar Formation|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
15764|Quilalar Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
15764|Quilalar Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1750Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
15764|Quilalar Formation|61922|5|Briefly described|p8, p9 Fig. 3|||Together with the Mitakoodi Quartzite and Ballara Quartzite a part of this unit forms a marker horizon within the cover sequence 2.  Geological Province: Mount Isa Inlier/Eastern Fold Belt.||||||
15764|Quilalar Formation|61925|5|Briefly described|p64|||Correlates with Mitakoodi Quartzite and Ballara Formation in the Eastern Fold Belt. Geological Province: Western Fold Belt, Mount Isa Inlier.||||||
15764|Quilalar Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
15764|Quilalar Formation|61936|5|Briefly described|p193|Paleoproterozoic|Paleoproterozoic|A shallow marine quartzite-carbonate succession. Overlies the Myally Group. Age: ca1755Ma. Geological Province: Leichhardt Superbasin, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|62084|5|Briefly described|p936 Fig.5|||Leichhardt Superbasin. Shown as Quilalar Fm.|1755+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
15764|Quilalar Formation|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Included in the Quilalar Supersequence spanning the interval ~1755-1740Ma (in the Western Succession). Geological Province: Mount Isa Inlier.||||||07-NOV-08
15764|Quilalar Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Ages: 1763+/-8Ma,1759+/-5Ma,1748+/-4Ma. Max.thick: 2km. Unconformable on Lochness Fm (Myally Subgp). Geol.Prov: Calvert Superbasin. Quartzite, very fine-gr.hummocky sandstone, siltstone, variably carbonaceous shale, dolostone. See also p1027 Tb.1, p1030||||||07-NOV-08
15764|Quilalar Formation|63109|6|Mentioned|p1108 Fig. 3|||Underlain by Lochness Formation. Geological Province: Leichhardt Superbasin. Consists of dolostone and dolomitic siltstone and shale.||||||30-SEP-08
15764|Quilalar Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Bigie Formation, underlain by Myally Subgroup. Thickness:~ 2000m. Age: 1748+/-4Ma. Geological Province: Leichhardt Superbasin. Consists of sandstone with siltstone, shale and very fine sandstone and undifferentiated dolostone.||||||07-FEB-11
15764|Quilalar Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Lochness Formation. Is overlain ?unconformably by Bigie Formation.||
15764|Quilalar Formation|63114|5|Briefly described|p1253 Fig.2. |||Leichhardt superbasin.||||Overlies Lochness Formation (Myally Subgroup). Is overlain by Bigie Formation.||
15764|Quilalar Formation|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
15764|Quilalar Formation|63116|6|Mentioned|p1297 Fig.2, |||Leichhardt superbasin. Material properties detailed.||||||
15764|Quilalar Formation|63593|5|Briefly described|p288 Fig.2, p291 Fig.3 and Tb.2.|||Western Fold Belt. 2000 m thick.|||||Sandstone, siltstone, shale, commonly calcareous.|
15764|Quilalar Formation|63866|5|Briefly described|p54, p56, p58|Statherian|Statherian|Leichhardt Superbasin.|1748 +/- 3 Ma (Neumann et al., 2006)|||Overlies the Bortala Formation.||
15764|Quilalar Formation|64248|6|Mentioned|p38 Fig.5|||Kalkadoon-Leichhardt Belt. Equivalent to Corella Formation and Ballara and Mitakoodi Quartzites.||||||11-DEC-17
15764|Quilalar Formation|64250|5|Briefly described|p25 fig 10, p11 fig 3, p22|||Widespread across Mt Isa Inlier deposited in NW-SE trending basin open to SE.  Detrital zircons consistent with Argylla and Bottletree Formations origin or from the NW, Nicholson Granite, Cliffdale Volcanics and Kamarga Volcanics.|<1748 +/- 4 Ma|||Overlies Haslingden Group, Myally Subgroup.  Correlated with Ballara Quartzite and Mitakoodi Quartzite.|Variably calcareous.|
15764|Quilalar Formation|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Ages: 1763+/-8Ma, 1748+/-4Ma.||||||07-FEB-11
15764|Quilalar Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
15764|Quilalar Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
15764|Quilalar Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
15764|Quilalar Formation|64834|5|Briefly described|p13 Fig.2|||Leichhardt Superbasin. Western Succession of Mount Isa Basin.|||||Sandstone; siltstone, shale, very fine sandstone; undifferentiated dolostone.|
15764|Quilalar Formation|65337|6|Mentioned|p5. |||Leichhardt Superbasin; Leichhardt River Fault Trough.||||||
15764|Quilalar Formation|65396|5|Briefly described|p16, p82, p175, p187, p190, p193-196|Statherian|Statherian|See also p201, p241. Leichhardt Superbasin. Cover Sequence 2. Leichhardt River Fault Trough, Kalkadoon Leichhardt Belt. Detrital zircon sources listed. Shallow-marine deposits.|1748 +/- 4 Ma (Neumann et al., 2005).|||Overlies Myally Subgroup (Haslingden Group). Correlated with Ballara and Mitakoodi Quartzites and Corella Formation.|Calcareous metasediments, sandstone, mafic and felsic volcanics.|
15764|Quilalar Formation|65505|6|Mentioned|980|Proterozoic|Proterozoic|Age: c.1750 Ma.||||||
15764|Quilalar Formation|66529|6|Mentioned|p32 |||Uppermost unit in Leichhardt Superbasin.|||||Fine-grained siliciclastics and dolostone.|
15764|Quilalar Formation|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1755 +/- 3 Ma (Page et al. 2000).|||||24-APR-12
15764|Quilalar Formation|67323|5|Briefly described|p11, p15, p24, p31, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt Superbasin. Mount Oxide, Leichhardt River and Century Domains, Mount Isa Inlier. The lower part is a clastic succession deposited during extension; the upper part is a sag-phase carbonate succession.|~1775-1750 Ma (lower); ~1750-1740 Ma (upper).|||Unconformably overlain by Surprise Creek Formation, Bigie Formation. Equivalent to Ballara Quartzite, Mitakoodi Quartzite and Corella Formation. Intruded by Kalkadoon Granite?|Feldspathic quartzite, orthoquartzite, conglomerate, feldspathic grit, shale, siltstone.|
15764|Quilalar Formation|68021|5|Briefly described|p135 fig 4, p138|Statherian|Statherian|Quilalar Supersequence, Leichhardt Superbasin, Western Succession. Fluviatile to shallow marine sediments.|~1755 - ~1740 Ma|||Overlies Myally Subgroup unconformably, overlain by Fiery Creek Volcanics, Bigie Formation unconformably. Intruded by Weberra Granite?|Clean, well-sorted quartzite, well-bedded stromatolitic limestones, redeposited calcareous sandstones.|
15764|Quilalar Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
15764|Quilalar Formation|68575|6|Mentioned|p107-108|||||||Nonconformably overlies Kalkadoon Granite.||
15764|Quilalar Formation|68732|5|Briefly described|p159-163, p165-167, p169, p171|Statherian|Statherian|Contains flat rhythmites. Of the Quilalar Supersequence. Rocks characterised by a transgressive-regressive cycle. Maximum sedimentary depositional ages.|1763 +/- 8, 1748 +/- 4 Ma||||Includes fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones; very fine-grained arkosic sandstones. Also sandstone-siltstone-shale laminae and thin beds (rhythmites).|01-DEC-17
15764|Quilalar Formation|69056|6|Mentioned|p2|||||||||
15764|Quilalar Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough. Post-rift subsidence deposits.||||Overlies Myally Subgroup, overlain by Bigie Formation, Fiery Creek Volcanics||09-FEB-18
15764|Quilalar Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Myally Subgroup.||25-JAN-19
15764|Quilalar Formation|69591|5|Briefly described|p29, p33-34, p38, p40, p57, p105-106|Paleoproterozoic|Paleoproterozoic|Part of the Quilalar Supersequence. Leichhardt River Domain. Probably absent N of the Murphy Tectonic Ridge. Shelf-fluvial shoreline deposits.|1748 +/- 4 Ma (MDA: Neumann et al., 2006).|||Equivalent to Corella Formation. ?Intruded by Augustus Igneous Complex.|Feldspathic quartzite, orthoquartzite, conglomerate, feldspathic grit, shale, siltstone.|
15764|Quilalar Formation|70282|6|Mentioned|p544 Tb.1|||Cover sequence 2, Mount Isa.|1790-1760 Ma (or 1720 Ma)|||||13-FEB-18
15764|Quilalar Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Nine facies are mapped separately.|||||Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1780+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone, basaltic andesite.|
15764|Quilalar Formation|71606|5|Briefly described|p137|Statherian|Statherian|Lawn Hill Platform, Mount Isa Inlier.||||Overlain unconformably by Bigie Formation. Underlain  by Myally Subgroup.||
15764|Quilalar Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1750 Ma|||Overlies the Myally Supergroup.|Sandstone, greywacke, dolomite and calc-silicate rocks.|
15764|Quilalar Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||||Shown as overlying Whitworth Formation and Argylla Formation.||
15764|Quilalar Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain and the Kalkadoon-Leichhardt Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||||Shown as equivalent to Stanbroke Sandstone, Mary Kathleen Group.|Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain and the Kalkadoon-Leichhardt Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||||Shown as equivalent to Stanbroke Sandstone, Mary Kathleen Group.|Feldspathic to quartzose sandstone, conglomerate, shale and siltstone, and minor limestone and dolomite.|
15764|Quilalar Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
15764|Quilalar Formation|72912|5|Briefly described|p5 Fig.3, p12.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.||||Correlated with Corella and Doherty Formations.||
15764|Quilalar Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||||Underlain by(?) Whitworth Quartzite (Myally Subgroup).||
15764|Quilalar Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
15764|Quilalar Formation|73413|6|Mentioned|p3|||Mount Isa Inlier.||||||
15764|Quilalar Formation|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13, p20|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1776+/-7 Ma, 1763+/-8 Ma, 1748+/-4 Ma MDA||||Clastics, includes mafic extrusives, carbonates.|
15774|Quita Formation|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Sequence of thin-bedded to laminated bituminous limestone with some irregular chert laminae and nodules. Erosional contact with overlying Steamboat Sandstone. Interfingers with the Blazan Shale. Geological Province: Georgina Basin.||||||
15774|Quita Formation|30242|6|Mentioned|Fig.2|||||||||
15774|Quita Formation|30479|6|Mentioned|Fig.6|||See also p19. Name should be dropped.||||||27-NOV-06
15774|Quita Formation|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15774|Quita Formation|33111|6|Mentioned|Fig.15|||||||||
15774|Quita Formation|34287|6|Mentioned|Fig.3|||||||||
15774|Quita Formation|35054|6|Mentioned|Table 23|||||||||
15774|Quita Formation|35139|6|Mentioned|p46|||||||||
15774|Quita Formation|35553|6|Mentioned|p47|||||||||
15774|Quita Formation|36234|6|Mentioned|p168|||||||||
15774|Quita Formation|37572|4|Described|p158|||See also Fig.8 and p165.||||||27-NOV-06
15774|Quita Formation|38442|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|||||||25-AUG-04
15774|Quita Formation|38446|6|Mentioned|Table 23|||||||||
15774|Quita Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
15774|Quita Formation|39445|5|Briefly described|Table 4|||See also p62.||||||27-NOV-06
15774|Quita Formation|39690|6|Mentioned|p88|||||||||
15774|Quita Formation|40038|6|Mentioned|p248|||||||||
15774|Quita Formation|44211|2|Defined|p93,96,100-107|||Rests on eroded surface of Middle Cambrian rocks.||||||
15774|Quita Formation|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
15774|Quita Formation|44275|14|Not recorded|Map Legend|||||||||
15774|Quita Formation|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
15774|Quita Formation|45012|14|Not recorded|p26,307|||Fauna.||||||
15774|Quita Formation|45052|3|Fully described|p100|||M.Camb.||||||
15774|Quita Formation|45054|6|Mentioned|p5|||Fossil locality||||||
15774|Quita Formation|45079|4|Described|p34|||Cambrian age||||||
15774|Quita Formation|45166|5|Briefly described|Table 15|||||||||
15774|Quita Formation|60122|6|Mentioned|p11 Tb. 1, p18|||Possibly disconformably overlain by Steamboat Sandstone?||||||
15774|Quita Formation|60123|5|Briefly described|p5|||Possibly disconformably underlies Steamboat Sandstone.||||||
15774|Quita Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Bituminous limestone, marl, mudstone; minor chert, sandstone.||||||
15774|Quita Formation|64068|4|Described|p63-64, 62, 65|Middle Cambrian|Middle Cambrian|Formerly included in Steamboat Sandstone (Reynolds, 1965). Contains trilobites, hyoliths, molluscs. Correlated with Arthur Creek Formation, Blazan Shale, Inca Formation, Roaring Siltstone, Devoncourt Limestone, Currant Bush Limestone, Age Creek Formation, Camooweal Dolostone.||Of Narpa Group.||Conformably overlies or interdigitates with Blazan Shale. Disconformable over Beetle Creek Formation or Thorntonia Limestone. Conformably (or disconformably?) overlain by Steamboat Sandstone.|Siliceous shale, marly and quartzic limestone with nodular chert.|05-APR-12
15774|Quita Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.|||Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
15774|Quita Formation|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
15774|Quita Formation|69573|6|Mentioned|p659, 665|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites. High energy, inner shelf setting.||||||
15774|Quita Formation|69591|5|Briefly described|p87, p91, p96|Cambrian|Cambrian|Ardmore/Quita Creek area, Oban Sub-basin, Georgina Basin. 60-70m thick.||||Disconformably overlies Blazan Shale. Is overlain by Steamboat Sandstone transitionally.|Light-grey to dark-grey, bituminous, thin-bedded to laminate limestone (fine calcarenite, calcilutite or oolitic), with regressive interbeds of grey to yellowish marl and mudstone with some irregular chert laminae and nodules.|
15774|Quita Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Blazan Shale. Is overlain by Steamboat Sandstone.||
15774|Quita Formation|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Toko Syncline, Georgina Basin.  Australian stages: Undillan to Boomerangian.||of Narpa Group.||||
15774|Quita Formation|72516|6|Mentioned|p92|||Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||
15784|Raceview Formation|12597|5|Briefly described|p491, p492 Tb.1, p494, p500, p501|Rhaetian|Rhaetian|Clarence-Moreton Basin. Contains the oldest coal seams identified in the Surat, Clarence-Moreton and Eromanga Basins.||Unit in Woogaroo Subgroup.|||Sub-labile to quartzose sandstone, siltstone and mudstone; minor thin coal seams.|
15784|Raceview Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
15784|Raceview Formation|22757|5|Briefly described|Table5,p10|Late Triassic|Late Triassic|Ipswich-Moreton Basin. 30 m.||||||
15784|Raceview Formation|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rhaetian|Of the Woogaroo Subgroup (Bundamba Group). Interbedded sandstone, siltstone, claystone. Max. thickness: 250m. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|22865|6|Mentioned|Fig.22.10ap318|||||||||
15784|Raceview Formation|23799|5|Briefly described|p46|Late Triassic|Late Triassic|Of Woogaroo Subgroup.  Overlain by Ripley Road Sandstone; overlies Aberdare Conglomerate.  Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|23811|5|Briefly described|Map Legend|Rhaetian|Rhaetian|Of Woogaroo Subgroup. Thinly interbedded, fine- to medium-grained, quartz-lithic and quartz sandstone, silty sandstone, grey to buff siltstone and claystone, carbonaceous siltstone, claystone, minor laminite, coaly bands.Geol:Prov: Clarence-Moreton Basin.||||||20-DEC-04
15784|Raceview Formation|23812|5|Briefly described|p35 Tb.4|Late Triassic|Late Triassic|Of Bundamba Group.  Maximum thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 140m.||||||
15784|Raceview Formation|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
15784|Raceview Formation|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|29385|6|Mentioned|p82|||Jurassic.||||||
15784|Raceview Formation|29386|6|Mentioned|p454|||Upper Triassic.||||||
15784|Raceview Formation|30086|5|Briefly described|p4|||Triassic age. Part of Bundamba Group.||||||
15784|Raceview Formation|30087|4|Described|p3|||Unit of Bundamba Group. See also p4.||||||17-SEP-18
15784|Raceview Formation|30302|6|Mentioned|p415|||Refers to Staines(1964)||||||
15784|Raceview Formation|30458|6|Mentioned|p1|||See also p40.||||||17-SEP-18
15784|Raceview Formation|30459|6|Mentioned|p309|||||||||
15784|Raceview Formation|30461|6|Mentioned|p100|||||||||
15784|Raceview Formation|30463|6|Mentioned|p466|||Palynology. See also p464,467,471.||||||17-SEP-18
15784|Raceview Formation|30464|6|Mentioned|p3|||||||||
15784|Raceview Formation|30465|6|Mentioned|p4|||||||||
15784|Raceview Formation|30466|6|Mentioned|p3|||||||||
15784|Raceview Formation|30470|6|Mentioned|p459|||||||||
15784|Raceview Formation|30471|6|Mentioned|p129|||Miospore assemblages listed in Appendix.||||||
15784|Raceview Formation|30472|6|Mentioned|p132|||Pollen distribution.||||||
15784|Raceview Formation|30474|6|Mentioned|p251|||Correlation chart on p251.||||||17-SEP-18
15784|Raceview Formation|30475|6|Mentioned|p160|||||||||
15784|Raceview Formation|30477|6|Mentioned|p461|||||||||
15784|Raceview Formation|30478|6|Mentioned|p461|||||||||
15784|Raceview Formation|30508|6|Mentioned|p87|||Mesozoic age. Redbank Plains form Station site||||||
15784|Raceview Formation|30517|6|Mentioned|p436|||||||||
15784|Raceview Formation|30565|6|Mentioned|p129|||||||||
15784|Raceview Formation|30701|6|Mentioned|Map legend|Triassic|Triassic|||||||
15784|Raceview Formation|30915|6|Mentioned|p100|||||||||
15784|Raceview Formation|30916|6|Mentioned|p99|||||||||
15784|Raceview Formation|31118|4|Described|p320|||||||||
15784|Raceview Formation|31259|6|Mentioned|p325|||Refers Staines (1964).||||||17-SEP-18
15784|Raceview Formation|32136|6|Mentioned|p5|||Miospores||||||
15784|Raceview Formation|32176|6|Mentioned|p2|||Bundamba Gp. See also p3, Figs. 2&3.||||||17-SEP-18
15784|Raceview Formation|32179|6|Mentioned|p3|||Trias.||||||
15784|Raceview Formation|32180|6|Mentioned|Table 1|||||||||
15784|Raceview Formation|32492|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
15784|Raceview Formation|32801|6|Mentioned|p266|||||||||
15784|Raceview Formation|32803|6|Mentioned|p95|||||||||
15784|Raceview Formation|33381|4|Described|p110|||See also pp115,117,118,122,Late Triassic. Map.||||||17-SEP-18
15784|Raceview Formation|33476|6|Mentioned|p99|||||||||
15784|Raceview Formation|34010|6|Mentioned|Cor. chart|||U.Triassic||||||
15784|Raceview Formation|34354|6|Mentioned|p3|||Triassic. See also p12.||||||17-SEP-18
15784|Raceview Formation|34457|6|Mentioned|p484|||Cor. with Borallon Beds||||||
15784|Raceview Formation|34505|6|Mentioned|p3|||Bundamba Group. See Figs.8,9,10,11||||||
15784|Raceview Formation|35079|6|Mentioned|p424|||||||||
15784|Raceview Formation|35101|6|Mentioned|p51|||||||||
15784|Raceview Formation|35901|6|Mentioned|p11|||||||||
15784|Raceview Formation|36237|6|Mentioned|Map legend|Late Jurassic|Late Triassic|Late Triassic to Early Jurassic||||||
15784|Raceview Formation|36243|6|Mentioned|Table 8A|||||||||
15784|Raceview Formation|36351|6|Mentioned|p373|||||||||
15784|Raceview Formation|36354|4|Described|p371|||||||||
15784|Raceview Formation|36779|6|Mentioned|p7|||||||||
15784|Raceview Formation|36825|6|Mentioned|p7|||||||||
15784|Raceview Formation|36899|6|Mentioned|p1085|||See also p1095.||||||17-SEP-18
15784|Raceview Formation|37111|6|Mentioned|Table 1|||||||||
15784|Raceview Formation|37122|5|Briefly described|Table 1|||||||||
15784|Raceview Formation|37375|4|Described|p474|||||||||
15784|Raceview Formation|37456|6|Mentioned|p268|||||||||
15784|Raceview Formation|37463|6|Mentioned|p483|||||||||
15784|Raceview Formation|37616|6|Mentioned|p33|||||||||
15784|Raceview Formation|37812|6|Mentioned|p657|||||||||
15784|Raceview Formation|38074|5|Briefly described|Table 1|||||||||
15784|Raceview Formation|38076|6|Mentioned|Table 3|||||||||
15784|Raceview Formation|38306|6|Mentioned|p509|||||||||
15784|Raceview Formation|38307|4|Described|p521|||||||||
15784|Raceview Formation|38441|6|Mentioned|Map legend|Rhaetian|Rhaetian|||||||
15784|Raceview Formation|39445|5|Briefly described|Table 10|||||||||
15784|Raceview Formation|39907|4|Described|p10|||Sedimentology||||||
15784|Raceview Formation|39943|6|Mentioned|Table 10A|||||||||
15784|Raceview Formation|40623|5|Briefly described|p32|||||||||
15784|Raceview Formation|41591|5|Briefly described|p19|||||||||
15784|Raceview Formation|41631|4|Described|p9|||See also Fig.2.||||||17-SEP-18
15784|Raceview Formation|41906|3|Fully described|Table 2 p16|||||||||17-SEP-18
15784|Raceview Formation|42248|6|Mentioned|p397|||||||||
15784|Raceview Formation|42316|6|Mentioned|p5|||||||||
15784|Raceview Formation|42336|5|Briefly described|Table 1 P5|||||||||
15784|Raceview Formation|42405|6|Mentioned|Table 3 P.7|||||||||
15784|Raceview Formation|42463|6|Mentioned|Fig.3 P170|||||||||
15784|Raceview Formation|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundamba Group).||||||15-JUL-04
15784|Raceview Formation|42869|5|Briefly described|Table 1, p33|||of Woogaroo Subgroup||||||17-SEP-18
15784|Raceview Formation|42893|5|Briefly described|Fig.2 p7|||||||||17-SEP-18
15784|Raceview Formation|42894|5|Briefly described|Fig.1 p20|||||||||17-SEP-18
15784|Raceview Formation|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Ipswich Basin.||||||12-APR-05
15784|Raceview Formation|43736|5|Briefly described|Table 1,p4|||||||||
15784|Raceview Formation|43910|14|Not recorded|p1,3,14,17,18,Fig.2|||||||||
15784|Raceview Formation|44450|5|Briefly described|p27|||Overlying unit Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|44633|14|Not recorded|p2|||||||||
15784|Raceview Formation|44734|14|Not recorded|p5,12,13,19|||Pine Mountain area.||||||
15784|Raceview Formation|44774|2|Defined|p30-32||Late Triassic|Conformable with both the overlying Ripley Road Sandstone and the underlying Aberdare Conglomerate.||||||
15784|Raceview Formation|44775|4|Described|p9||Late Triassic|||||||
15784|Raceview Formation|44776|14|Not recorded|p4,fig.3||Late Triassic|||||||
15784|Raceview Formation|44884|4|Described|p2,3,Figs.1,7|||||||||
15784|Raceview Formation|44885|14|Not recorded|p2,3|||||||||
15784|Raceview Formation|45110|3|Fully described|p82|||See also Table 17.||||||
15784|Raceview Formation|48917|5|Briefly described|p13|||See Table 2. Upper Triassic||||||
15784|Raceview Formation|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Sandstone, siltstone, claystone, conglomerate and minor coal.||||||
15784|Raceview Formation|60281|5|Briefly described|p27, p30, Fig. 18 App. 1|Late Triassic|Late Triassic|Of Woogaroo Subgp (Bundamba Gp).  Shale, siltstone and sst., giving way to a quartz sandstone-dominated sequence, the overlying Ripley Road Sandstone; overlies Laytons Range Conglom., Ipswich C.M.  Max. thick: 250m.  Geol.Prov: Clarence-Moreton Basin.||||||27-APR-05
15784|Raceview Formation|60993|4|Described|p4, p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Mixed labile to quartsoze sst and shale sequence of interbedded sandstone, siltstone, shale; minor coal. Unconformably overlies Evans Head Coal Measures. Geol.Prov: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60995|4|Described|p59, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp. Was correlated with "Mill Creek Siltstone". Overlain by Ripley Road Sst; overlies Laytons Range Congom; Evans Head Coal. Mes. (which may be misidentified Raceview Fm).  Max. thick: 250m.  Geol. Prov: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60996|5|Briefly described|p72, p81|||Overlain by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60997|5|Briefly described|p139 Fig. 1|Rhaetian|Rhaetian|Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
15784|Raceview Formation|60999|5|Briefly described|p164, p176|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Overlies the Laytons Range Conglomerate in several boreholes in NSW. Geological Province: Clarence-Moreton Basin. See also p169, p172 Fig. 6..||||||
15784|Raceview Formation|61002|5|Briefly described|p202|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.  See also p199 Fig. 3.||||||
15784|Raceview Formation|61004|5|Briefly described|p232 Fig. 2|Triassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|61005|5|Briefly described|p239, p242|||Geological Province: Clarence-Moreton Basin. See also p255 Figs. 23, 24 and 25.||||||
15784|Raceview Formation|61006|5|Briefly described|p277, p289|Triassic|Triassic|Mudstone, sandstone, composition variable. Some good hydrocarbon shows. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p286.||||||
15784|Raceview Formation|61310|5|Briefly described|p21, Table C1 (p22-23)|||Of the Woogaroo Subgroup. Pebble/cobble conglomerate, minor sandstone. Geological Province: Clarence-Moreton Basin||||||
15784|Raceview Formation|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
15784|Raceview Formation|64665|5|Briefly described|p53 Fig.2, p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin. Fluvio-lacustrine deposits.||Unit in Woogaroo Subgroup.||Overlies Aberdare and Laytons Range Conglomerates. Is overlain by Ripley Road Sandstone.|Includes thin coal seams.|
15784|Raceview Formation|64856|6|Mentioned|p80|Rhaetian|Norian|Moreton Basin. Base of Bundamba Group.|| ||||29-NOV-17
15784|Raceview Formation|67402|4|Described|p165 tbl LPB1, p187|Norian|Norian|Clarence-Moreton Basin. Deposited in a fluvial system with suspended load channels. Approximately 100m thick. Sandstones are often reservoirs and potential reservoirs for the storage of carbon dioxide. See also p188, p190 fig CLM6, p192, p193, p223, p225.||Woogaroo Subgroup||Overlies the Aberdare and Laytons Range Conglomerates. Overlain by the Ripley Road Sandstone.|Interbedded sandstone, siltstone and claystone with minor coal deposits.|
15784|Raceview Formation|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. Between 1-250m thick. Potential reservoir rock.||Woogaroo Subgroup||Overlies the Laytons Range Conglomerate. Overlain by the Ripley Road Sandstone.||
15784|Raceview Formation|69594|5|Briefly described|p519, p524, p534, p543-544,p546-547,p572|Late Triassic|Late Triassic|Clarence-Moreton Basin. Generally poorly outcropping.||Woogaroo Subgroup.||Overlies Aberdare Conglomerate (=Laytons Range Conglomerate in NSW); both are equivalent to the Eddystone beds. Is overlain by Ripley Road Sandstone. Equivalent to Eddystone beds.|Mudstone and siltstone predominate over sandstones (mostly feldspathic lithic and lithic); few minor conglomerates; cross-bedding and ripple cross-laminations fairly common.|
15784|Raceview Formation|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Northern Clarence-Moreton Basin area.||||||
15784|Raceview Formation|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Shown as including Aberdare Conglomerate member.||Woogaroo Subgroup.||Is overlain by Ripley Road Sandstone.||
15784|Raceview Formation|72297|5|Briefly described|p700|||Clarence-Moreton Basin.||||Equivalent to Tiaro Coal Measures.||
15784|Raceview Formation|73570|6|Mentioned|p912 Fig.2|||||||Overlies Laytons Range Conglomerate||
15803|Raglan Limestone|31519|6|Mentioned|p916|||||||||
15803|Raglan Limestone|31659|6|Mentioned|p28|||Refers Jack & Etheridge (1892)||||||
15803|Raglan Limestone|46803|6|Mentioned|p148|||||||||
15803|Raglan Limestone|50190|5|Briefly described|p38|Middle Devonian|Early Devonian|Of the Mount Holly beds. Interbedded with shales. On the BAJOOL 1:100k sheet.||||||13-JAN-05
15807|Rainbow Creek beds|24076|5|Briefly described|p397 Fig. 2|Late Permian|Late Permian|Max. thickness: 1525m.  Geological Province: Yarrol Basin.||||||
15807|Rainbow Creek beds|38153|6|Mentioned|p368|||||||||
15807|Rainbow Creek beds|39252|5|Briefly described|p21|||see also P27||||||
15807|Rainbow Creek beds|41246|6|Mentioned|Map legend|Permian||||||||
15807|Rainbow Creek beds|42370|5|Briefly described|Fig.3 P317|||||||||
15817|Rammutt Formation|23251|5|Briefly described|Table 1 p14, p19||Early Permian|Replaced Upper and Lower Nash Clastics of Arnold (1996).  Both plant and shelly macrofossil assemblage indicate an Early Permian age. Gympie Group. Kin Kin Subprovince, Gympie Province. Underlies South Curra Limestone;  overlies Highbury Volcanics.||||||21-JUN-06
15817|Rammutt Formation|23542|4|Described|Table 1 p379.|||Of the Gympie Group.||||||24-SEP-08
15817|Rammutt Formation|23799|5|Briefly described|p32|Early Permian|Early Permian|See also Rammut Formation.  Of the Gympie Group.  Geological Province: Kin Kin Subprovince (Gympie Province).||||||
15817|Rammutt Formation|30450|6|Mentioned|Table 1|||Permian age. Maryborough Basin||||||
15817|Rammutt Formation|31703|6|Mentioned|Table|||P4||||||
15817|Rammutt Formation|32945|6|Mentioned|p88|||Permian||||||
15817|Rammutt Formation|34475|2|Defined|p250|early Artinskian|early Artinskian|See also PP247,266,267Prob.Lower Artinskian.||||||24-SEP-08
15817|Rammutt Formation|35101|6|Mentioned|p22|||P26||||||
15817|Rammutt Formation|35284|6|Mentioned|p43|||||||||
15817|Rammutt Formation|36045|6|Mentioned|p332|||||||||
15817|Rammutt Formation|36926|6|Mentioned|p160|||||||||
15817|Rammutt Formation|39252|6|Mentioned|p22|||See also Fig.13||||||
15817|Rammutt Formation|39284|5|Briefly described|p431|||||||||
15817|Rammutt Formation|39445|5|Briefly described|Table 8|||||||||
15817|Rammutt Formation|41157|5|Briefly described|p81|||||||||
15817|Rammutt Formation|41272|5|Briefly described|M 1of1 D16|||See also M 1of1 N15||||||
15817|Rammutt Formation|41917|6|Mentioned|p521|||||||||
15817|Rammutt Formation|42344|5|Briefly described|p59|||||||||
15817|Rammutt Formation|42450|4|Described|p404|||||||||
15817|Rammutt Formation|42751|4|Described|p24|||Of Gympie Group.||||||24-SEP-08
15817|Rammutt Formation|43006|4|Described|Table 1,p239|||||||||
15817|Rammutt Formation|43017|5|Briefly described|Fig.3,p375|||||||||
15817|Rammutt Formation|43018|6|Mentioned|p392|||||||||
15817|Rammutt Formation|43100|4|Described|p20|||Of Gympie Group.||||||24-SEP-08
15817|Rammutt Formation|44925|5|Briefly described|Map Legend||Permian|||||||
15817|Rammutt Formation|44928|5|Briefly described|Map Legend||Permian|||||||
15817|Rammutt Formation|50320|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Gympie Province||||||
15817|Rammutt Formation|61772|6|Mentioned|p128||Early Permian|In New England Orogen.||||||24-SEP-08
15817|Rammutt Formation|61780|4|Described|p256, p257|Middle Permian|Early Permian|Thickness: >760m. Includes; Top Conglomerate, Nash Clastics, Pengelly Siltstone, Calton Volcanics, Calton Clastics.||||||
15817|Rammutt Formation|65380|5|Briefly described|p660 Table 1, p670, 671, p672 Table 3|Kungurian|Artinskian|Gympie Terrane.  Maximum depositional age from detrital zircon: 276 +/-2 Ma. Artinskian fossils in upper part.||||Overlain by South Curra Limestone. Upper part also known informally as Pengelly Siltstone.|Volcaniclastic sandstone.|
15817|Rammutt Formation|68111|5|Briefly described|p979|Early Permian|Early Permian|Gympie Terrane. Maximum age of 276 +/- 2 Ma determined from detrital zircons (Korsch et al. 2009).||||||22-OCT-14
15817|Rammutt Formation|68679|5|Briefly described|p326, p369-370, p470|Sakmarian|Asselian|Runnegar and Ferguson (1969). Southern Gympie Province. A number of authors (listed) have recognised six subdivisions within this unit, but they are not significant outside the Gympie goldfield. Up to 760m thick. Calc-alkaline andesites.||Gympie Group.||Correlated with Kolbar Formation.|Upper unit of coarse, well-rounded pebble conglomerate with gritty sandstone lenses; unconformable on an amygdaloidal olivine-bearing alkaline dolerite sill; andesite, basalt, polymict conglomerate, sandstone, minor carbonaceous mudstone.|
15817|Rammutt Formation|70913|4|Described|p1, 2, 9-10, 24-60, p8 fig 3, App 1 maps|Permian|Permian|Said to be redefined? Gympie Province. Type section mentioned and briefly described. Consistuent units discussed in detail. See also p67 fig 9, p77.||Gympie Group|Includes from base to top the Eldorado Clastics, Calton Andesite, Nash Clastics, Pengelly Siltstone and Glanmire Conglomerate Members.|Overlies the Mary Basalt. Overlain by the South Curra Limestone.|Volcanogenic sandstone, grey-green shale, argillite, conglomerate, siltstone and andesite.|28-FEB-19
15817|Rammutt Formation|72037|4|Described|p859,861-864,868-871|Middle Permian|Early Permian|Geological province: New England Orogen, Gympie Terrane. Zircon age spectrum with ~276 Ma peak, and clusters at 318 Ma and 330 Ma (Korsch et al., 2009a), interpreted to have been sourced from New England Orogen during accretion of Gympie Terrane onto the Australian margin. LA-ICP-MS peak detrital zircon U-Th-Pb ages includes 265 Ma and 312 Ma from the Calton Clastics, and 302, 345, 384, 427 and 505 Ma from the Alma Formation. Artinskian fossil assemblages described by Runnegar and Ferguson 1969 restrict depositional age to early-middle Permian (290-265 Ma). Late Permian to Triassic detrital zircons likely sourced from a middle Permian to Triassic continental arc system to the west, which was built on the former accretionary complex of the New England Orogen Gust et al., 1993; Bryant et al., 1997; Holcombe et al., 1997b; Li et al., 2012b). Carboniferous-age zircons correspond to detritus eroded from a Carboniferous magmatic arc of the New England Orogen, or recycled through the Carboniferous fore-arc and accretionary complex rocks.|||Includes Pengelly Siltstone, and Nash, Calton and Hall clastics, Calton, Mary and Tozer volcanics, and Alma Formation.|Overlain conformably by South Curra Limestone. Underlain disconformably to unconformably by Highbuy Volcanics.||
15817|Rammutt Formation|72297|5|Briefly described|p758|||Near Gympie, the colour-banded tuff, locally termed "Gympieite", is promoted as a semiprecious gemstone.|||||Green and blue banded, cherty dacitic tuff.|
15817|Rammutt Formation|73197|5|Briefly described|p472, p474, p477 Tb.3, p478|Lopingian|Cisuralian|New England Orogen, northern. Detrital zircons indicate a New England Orogen provenance (Li et al., 2015). Includes plant fossils as well as geochemical and isopotic characteristics indicating some continental affinity (Sivell and McCulloch, 2001). Age range of 275-255 Ma for the Calton Andesite Member constituent unit.|276 Ma, 295-265 Ma, 275-255 Ma|Gympie Volcanics|Calton Clastics, Calton Andesite Member|Overlies the Highbury Volcanics.|Andesitic and minor dacitic volcanics. Includes volcaniclastic granule conglomerate containing sandstone.|
15817|Rammutt Formation|73303|5|Briefly described|p61 Fig.2, p62, p69 Fig.9|Cisuralian|Cisuralian|New England Orogen. Gympie Terrane, southern. Brachiopod assemblage correlative with Kolbar Formation. Misspelt as Rummutt Fm p68.|276 Ma detrital zircon maximum depositional age|||Overlies Mary Basalt, underlies South Curra Limestone.|Dominated by fine- to coarse-grained volcaniclastic rocks.|
15828|Rands Formation|30451|4|Described|p32|||||||||
15828|Rands Formation|30668|6|Mentioned|p582|||Occurrence of Septatopora pustulosa (Crockford).||||||
15828|Rands Formation|30772|6|Mentioned|p5|||Refers Maxwell (1964)||||||
15828|Rands Formation|31659|6|Mentioned|Table 2|||Correlation||||||
15828|Rands Formation|32141|6|Mentioned|p153|||||||||
15828|Rands Formation|32868|6|Mentioned|p202|||||||||
15828|Rands Formation|32945|6|Mentioned|Fig.1|||Permian||||||
15828|Rands Formation|33774|6|Mentioned|p23|||Stratigraphy||||||
15828|Rands Formation|33992|6|Mentioned|p237|||M.Carb.  See also P238||||||
15828|Rands Formation|34085|6|Mentioned|Cor.chart|||Stephanian||||||
15828|Rands Formation|34132|6|Mentioned|p2|||Upper Carboniferous||||||
15828|Rands Formation|35492|6|Mentioned|p145|||||||||
15828|Rands Formation|36528|6|Mentioned|p174|||||||||
15828|Rands Formation|36794|6|Mentioned|p386|||||||||
15828|Rands Formation|39252|6|Mentioned|Fig.11|||||||||
15828|Rands Formation|39267|6|Mentioned|p253|||||||||
15828|Rands Formation|39445|5|Briefly described|Table 7 p98|||||||||
15828|Rands Formation|39632|6|Mentioned|p224|||||||||
15828|Rands Formation|40093|6|Mentioned|p36|||||||||
15828|Rands Formation|42547|4|Described|p52|||||||||
15828|Rands Formation|43474|14|Not recorded|p25,90||Late Carboniferous|||||||
15828|Rands Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
15828|Rands Formation|43983|14|Not recorded|p1-3|||||||||
15828|Rands Formation|44091|14|Not recorded|p37,Tb.3,p47||Late Carboniferous|||||||
15828|Rands Formation|44360|2|Defined|p1-3,16-21,23-28,||Stephanian|p30-32,35,map. Unit of Boiling Creek Group.||||||
15828|Rands Formation|44369|2|Defined|p169-170|||Greywacke, arkose.||||||
15828|Rands Formation|44370|14|Not recorded|p219,Tb.7|||||||||
15828|Rands Formation|44372|6|Mentioned|p5-7||Late Carboniferous|Overlies Poperima Formation. Underlies Burnett Formation.||||||
15828|Rands Formation|44515|2|Defined|p30||Late Carboniferous|Fossils||||||
15828|Rands Formation|44874|14|Not recorded|p102|||||||||
15828|Rands Formation|45031|14|Not recorded|p69,72||Late Carboniferous|||||||
15828|Rands Formation|45097|5|Briefly described|Fig.|||?date of boundary. Correlation chart.||||||
15828|Rands Formation|68008|5|Briefly described|p120, p596|Late Carboniferous|Late Carboniferous|Maxwell (1959, 1960, 1964). Yarrol and Cannindah areas. Combined with Burnett Formation by Brown (1970) and Edwards (1974) but without a new stratigraphic name. Subsequently subsumed into the Lorray Formation. Contained Myonia pollocki fossils.||Boiling Creek Group.||||
15828|Rands Formation|68679|5|Briefly described|p341|||Maxwell (1964). Cannindah area. Superseded; assigned to Boiling Creek Group by McKellar (1967) which itself is (?being) replaced by Lorray Formation. Contains a late Asselian fauna.||Boiling Creek Group.||||
15841|Ranmoor Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province.||||||
15841|Ranmoor Member|23982|5|Briefly described|p58 Fig.18|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|30020|6|Mentioned|p33|||||||||
15841|Ranmoor Member|30024|6|Mentioned|p332|||||||||
15841|Ranmoor Member|30042|6|Mentioned|p5|||Tambo faunas correlation.||||||
15841|Ranmoor Member|30443|6|Mentioned|p14|||Albian age||||||
15841|Ranmoor Member|31208|6|Mentioned|p48|||||||||
15841|Ranmoor Member|32314|6|Mentioned|Fig. 4|||||||||
15841|Ranmoor Member|33016|6|Mentioned|p1|||On table||||||
15841|Ranmoor Member|33017|6|Mentioned|p6|||||||||
15841|Ranmoor Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
15841|Ranmoor Member|33175|5|Briefly described|p280|||||||||
15841|Ranmoor Member|33182|6|Mentioned|Table 1|||L.Cret.||||||
15841|Ranmoor Member|33368|6|Mentioned|p25|||Strat. table.||||||
15841|Ranmoor Member|33414|6|Mentioned|p212,Tb.||Cretaceous|Part of Wallumbilla Formation.||||||
15841|Ranmoor Member|33638|5|Briefly described|Table 1|||||||||
15841|Ranmoor Member|33640|6|Mentioned|p12|||||||||
15841|Ranmoor Member|33642|6|Mentioned|144,147-8,Tb.1,Fig.2|||Refers Vine & Day(1965). Lower part-Lower Albian fauna, upper part has possible Middle Albian fossils.||||||
15841|Ranmoor Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33648|6|Mentioned|p21|||Strat.||||||
15841|Ranmoor Member|34091|5|Briefly described|Table 1|||L.Cret||||||
15841|Ranmoor Member|35239|6|Mentioned|p265|||||||||
15841|Ranmoor Member|35560|6|Mentioned|p291|||||||||
15841|Ranmoor Member|35793|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|35811|6|Mentioned|p556|||Exploration carried out.||||||
15841|Ranmoor Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
15841|Ranmoor Member|36552|6|Mentioned|p61|||||||||
15841|Ranmoor Member|36571|6|Mentioned|Table 4|||||||||
15841|Ranmoor Member|38199|6|Mentioned|p428|||See also P429.||||||
15841|Ranmoor Member|38814|6|Mentioned|Table 1|||||||||
15841|Ranmoor Member|39211|5|Briefly described|Fig.3|||See also Figs 9,11,12 etc.Correlation||||||
15841|Ranmoor Member|40801|6|Mentioned|p46|||||||||
15841|Ranmoor Member|40926|6|Mentioned|Table 2|||||||||
15841|Ranmoor Member|41086|3|Fully described|Fig.3|||||||||
15841|Ranmoor Member|41088|6|Mentioned|p141|||||||||
15841|Ranmoor Member|41266|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|44082|6|Mentioned|p10,18-20,Tb.p34||Albian|(Early Albian) Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
15841|Ranmoor Member|44087|14|Not recorded|p4,opp.7|||||||||
15841|Ranmoor Member|44089|14|Not recorded|Tb.1,p4||Early Cretaceous|(Wilgunya Formation)||||||
15841|Ranmoor Member|44346|14|Not recorded|p4,opp.p5||Aptian|?Aptian||||||
15841|Ranmoor Member|44352|14|Not recorded|Map Legend||Early Cretaceous|||||||
15841|Ranmoor Member|44373|14|Not recorded|p20|||Map only.||||||
15841|Ranmoor Member|44374|14|Not recorded|p12|||Albian in lower part, highly mudstone sequence, with carbonaceous interval, equivalent to non-marine Coreena Member.||||||
15841|Ranmoor Member|44406|14|Not recorded|p4,opp.p6|||Member of Wilgunya Formation.||||||
15841|Ranmoor Member|44408|14|Not recorded|p4,opp.p6||Aptian|||||||
15841|Ranmoor Member|44414|14|Not recorded|p110-112,114||Cretaceous|Correlated with Coreena Member.||||||
15841|Ranmoor Member|44417|2|Defined|p416,418-420||Albian|(Early Albian)||||||
15841|Ranmoor Member|44915|14|Not recorded|p18||Early Cretaceous|Ref. to Vine and Day 1965.||||||
15841|Ranmoor Member|45132|6|Mentioned|p11|||||||||
15841|Ranmoor Member|45145|6|Mentioned|p61|||||||||
15841|Ranmoor Member|46791|6|Mentioned|p44|||||||||
15841|Ranmoor Member|46937|6|Mentioned|Fig.10|||||||||
15841|Ranmoor Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
15841|Ranmoor Member|48920|6|Mentioned|p60|||See also Table 8. Refers Vine & Day (1965)||||||
15841|Ranmoor Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
15841|Ranmoor Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
15841|Ranmoor Member|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Of Wallumbilla Formation. Overlies Jones Valley Member. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
15841|Ranmoor Member|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in Queensland.||||
15841|Ranmoor Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Cretaceous|Cretaceous|Eromanga/Carpentaria Basins.||Wallumbilla Formation.|||Mudstone, commonly carbonaceous, minor siltstone.|
15841|Ranmoor Member|67784|5|Briefly described|p25-26, p28 Tb.1, p29, p31-33|Albian|Aptian|60-95m thick. Northern Eromanga Basin.||Wallumbilla Formation||Paraconformably overlies Jones Valley Member. Is overlain by Toolebuc Formation.||08-FEB-18
15841|Ranmoor Member|68206|5|Briefly described|p32-33|Albian|Albian|NE Eromanga Basin.||Wallumbilla Formation.||Overlies Jones Valley Member. Is overlain by Toolebuc Formation.||
15841|Ranmoor Member|69457|6|Mentioned|p41:10|||Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
15841|Ranmoor Member|69594|4|Described|p522, p526, p528|Albian|Albian|Vine and Day (1965). Eromanga Basin. The type section is near Glendower Station, E of Hughenden. Crops out in a discontinuous band from Glendower to NW of Richmond. No equivalent units have been identified. Thickness generally 60-95m; may be up to 312m. Contains early Albian ammonite, bivalves and belemnites.||Wallumbilla Formation.||Conformably overlies Jones Valley Member.|Dominated by mudstone and siltstone, with minor labile sandstone.|
15841|Ranmoor Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
15841|Ranmoor Member|72297|5|Briefly described|p753|||Eromanga Basin.||Wallumbilla Formation.||Is overlain conformably by the Toolebuc Formation.|Blue shale.|
15841|Ranmoor Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD).||Wallumbilla FZ.||Overlies Jones Valley Member. Is overlain by Toolebuc FZ.||
15867|Ravenshoe Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 307 +/- 4Ma, Rb-Sr.||||||
15867|Ravenshoe Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 419. I-Type.||||||
15867|Ravenshoe Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite||||||
15867|Ravenshoe Granite|40743|6|Mentioned|p318|||||||||
15867|Ravenshoe Granite|43259|4|Described|Appendix 1,p46.||Carboniferous|||||||
15867|Ravenshoe Granite|60425|4|Described|p286-7 Appdx.|Late Carboniferous|Late Carboniferous|Of Ravenshoe Suite (O'Briens Creek Supersuite). Ages: 307+/-4Ma and 309Ma (Rb-Sr). Pink, medium-grained biotite granite. I-type.||||||07-FEB-11
15914|Razorback beds|24491|5|Briefly described|p25|||||||||
15914|Razorback beds|24571|6|Mentioned|p15, 21|||||||||
15914|Razorback beds|35952|6|Mentioned|Fig.1|||||||||
15914|Razorback beds|38084|5|Briefly described|Fig.13|||||||||
15914|Razorback beds|38153|6|Mentioned|p364|||||||||
15914|Razorback beds|38373|6|Mentioned|p617|||||||||
15914|Razorback beds|40180|6|Mentioned|Fig.2|||||||||
15914|Razorback beds|41246|6|Mentioned|Map legend|Jurassic||||||||
15914|Razorback beds|41576|4|Described|p19|||See also Table 1||||||
15914|Razorback beds|41577|6|Mentioned|Map legend|Triassic||||||||
15914|Razorback beds|41922|4|Described|Table 1 P9|||||||||
15914|Razorback beds|41926|5|Briefly described|p52|||||||||
15914|Razorback beds|41983|6|Mentioned|Fig.1P1807|||||||||
15914|Razorback beds|68008|5|Briefly described|p228, p230, p261|Jurassic|Jurassic|See Rands (1892), Maitland (1895), Dunstan (1898), who wrongly interpreted these rocks to overlie the Stanwell Coal Measures. See also Staines (1953), for Jurassic sandstones in the Rockhampton 250k sheet area (Mount Morgan district). Described in detail by Playford and Cornelius (1967). Now included in the Precipice Sandstone.|||||Interbedded sandstone, mudstone, siltstone and conglomerate, overlain by cross-bedded sandstone with thin silty and shaly bands.|
15914|Razorback beds|68135|5|Briefly described|p52 Fig.2b, p64|Sinemurian|Hettangian|Surat Basin (QLD). Contains vertebrate tracks and body fossils, including the freshwater plesiosaur Siderops.
|||||Predominantly sandstone.|15-SEP-17
15914|Razorback beds|69594|5|Briefly described|p535, p551|Early Jurassic|Early Jurassic|Playford and Cornelius (1967). Mount Morgan and Stanwell areas. Recognised as outliers of the Precipice Sandstone.||||||
15914|Razorback beds|72297|5|Briefly described|p726|Early Jurassic|Early Jurassic|Landscape through to restoration-grade sandstone is quarried at Stanwell, W of Rockhampton.||Precipice Sandstone.|||Sandstone in a variety of colours.|
15914|Razorback beds|72921|5|Briefly described|p15 Fig.2.|Early Jurassic|Triassic|Shown as located in the Surat Basin in Queensland.||||Shown as partially underlying Evergreen Formation||
15930|Red Cliff Coal Measures|22857|4|Described|p284, p542 A.1 Tb.A1.11|Jurassic|Early Triassic|Lithic conglomerate and breccia, sandstone, siltstone, coal. Max. thickness: >100m. Geological Province: Ipswich Basin (under Clarence-Moreton Basin). See also p318-9 Figs. 22.10A,B.||||||
15930|Red Cliff Coal Measures|22860|6|Mentioned|Fig20.2p278|||||||||
15930|Red Cliff Coal Measures|22861|5|Briefly described|p284-85|||||||||
15930|Red Cliff Coal Measures|23811|5|Briefly described|Map Legend|Norian|Norian|Thin-bedded, to laminated carbonaceous claystone and siltstone, interbedded with lenses and beds of pebble-granule conglom. and breccia; minor carbonaceous, fine-grained lithic sandstone. Geological Province: Clarence-Moreton Basin.||||||22-SEP-05
15930|Red Cliff Coal Measures|23812|5|Briefly described|P31, p35 Tb.4|Late Triassic|Late Triassic|Together with Evans Head Coal Measures considered to be equivalent to the Ipswich Coal Measures. Maximum thickness: 600m.  Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|30784|6|Mentioned|p71|||List fossil megalforas found||||||
15930|Red Cliff Coal Measures|30785|6|Mentioned|p397|||||||||
15930|Red Cliff Coal Measures|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|32838|6|Mentioned|p320|||||||||
15930|Red Cliff Coal Measures|32916|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|33476|6|Mentioned|p99|||||||||
15930|Red Cliff Coal Measures|34340|2|Defined|p463|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|36327|6|Mentioned|p10|||||||||
15930|Red Cliff Coal Measures|37112|5|Briefly described|Table 1|||||||||
15930|Red Cliff Coal Measures|40245|6|Mentioned|Fig.2|||||||||
15930|Red Cliff Coal Measures|41550|3|Fully described|p491|||||||||
15930|Red Cliff Coal Measures|41591|6|Mentioned|Fig.1|||||||||
15930|Red Cliff Coal Measures|41631|4|Described|p4|||See also Fig.2||||||
15930|Red Cliff Coal Measures|42248|6|Mentioned|Fig2 P399|||||||||
15930|Red Cliff Coal Measures|43001|5|Briefly described|Fig.1,p118|||||||||
15930|Red Cliff Coal Measures|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
15930|Red Cliff Coal Measures|43383|14|Not recorded|p24|||||||||
15930|Red Cliff Coal Measures|43384|14|Not recorded|Map Legend||Triassic|||||||
15930|Red Cliff Coal Measures|43468|14|Not recorded|Map Legend||Triassic|Provisional Edition||||||
15930|Red Cliff Coal Measures|43881|2|Defined|p6-7,27-8,80-3,103,||Triassic|p105-6,142.||||||
15930|Red Cliff Coal Measures|44093|5|Briefly described|p72|Late Triassic|Late Triassic|See also p73 Fig. 7.3. Geological Province: Ipswich Basin.||||||
15930|Red Cliff Coal Measures|44450|5|Briefly described|p26|Late Triassic|Late Triassic|Overlain by Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||19-FEB-08
15930|Red Cliff Coal Measures|60281|5|Briefly described|p21-22, p25|||Geological Province: Ipswich Basin, Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|60993|5|Briefly described|p6 Fig. 2, p8|||Of McElroy (1963). Same unit as McTaggart's Esk beds (1963). Superseded by Ipswich Coal Measures.||||||
15930|Red Cliff Coal Measures|60997|5|Briefly described|p140 Fig. 2|||Of McElroy (1963).||||||
15930|Red Cliff Coal Measures|61001|6|Mentioned|p190 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61002|5|Briefly described|p196 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61006|6|Mentioned|p278 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61310|5|Briefly described|p16, Table C1 (p22-23)|Late Triassic|Late Triassic|Consist of conglomerate, lithic sandstone, siltstone, mudstone and coal. Max. thickness: ~600m. Geological Province: Clarence-Moreton Basin.  Along with Evans Head Coal Measures are equivalent to Ipswich Coal Measures. See also p15||||||23-JUN-06
15930|Red Cliff Coal Measures|61772|6|Mentioned|p130 Fig. 5||Late Triassic|Coal Measures is C.M. in text.||||||24-SEP-08
15930|Red Cliff Coal Measures|66855|6|Mentioned|p955.|Late Triassic|Late Triassic|||||||
15930|Red Cliff Coal Measures|68111|6|Mentioned|p966 Fig.1|||Ipswich Basin.||||||
15930|Red Cliff Coal Measures|68679|5|Briefly described|p388, p392|Late Triassic|Late Triassic|||||Equivalent to the Ipswich Coal Measures.||
15955|Red Mountain Formation|39445|5|Briefly described|Table 14|||||||||
15955|Red Mountain Formation|43029|5|Briefly described|p23|||||||||
15955|Red Mountain Formation|43204|5|Briefly described|Map Legend|Miocene|Tertiary|||||||23-DEC-11
15955|Red Mountain Formation|43213|4|Described|p10, p160-163, p238|Miocene|Oligocene|Grimes et al.(1980); originally "Red Mountain Beds" (Robertson, 1974) after the type locality at Red Mountain, N of Rubyvale. Crops out as isolated mesas. Early to Mid-Tertiary. 15-30 m thick. Unfossiliferous.||||Overlies Fork Lagoons beds, Anakie Metamorphic Group, Kettle Conglomerate Member.|Coarse, angular, consolidated gravels with a silty to quartzofeldspathic sandy matrix that locally contains detrital muscovite. Deeply wsaeathered , lateritised towards the top, and overlain by ferricrete.|
15955|Red Mountain Formation|60369|5|Briefly described|Map Legend|Tertiary|Tertiary|Clayey polymict conglomerate, sandstone, sandy claystone.||||||02-SEP-04
15955|Red Mountain Formation|61155|5|Briefly described|p20|Early Miocene|Late Oligocene|Overlies the Nebo Basalts, Peak Range and Emerald Volcancs and Hoy Basalt Plugs. Thickness: 15m. In the Fitzroy region.||||||
15955|Red Mountain Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
15955|Red Mountain Formation|69599|5|Briefly described|p580, p593|Miocene|Oligocene|Robertson (1974, 1983) and others. Occurs in a series of discrete, elongate packages N and NE of Rubyvale. Up to 30m thick. Lateritised in the Neogene.||||Unconformably overlies Kettle Conglomerate Member (Aldebaran Sandstone), Fork Lagoons beds, Kilmarnock Granodiorite, Annmore Quartz Monzodiorite, Silver Hills Volcanics and Telemon Formation.|Clayey conglomerate, pebbly sandstone and claystone. The (Permian) gravels are polymict, containing clasts of metamorphics, granitoids, silcrete and other fragments. Highly lateritised.|
15955|Red Mountain Formation|70856|5|Briefly described|Map Legend|Tertiary|Tertiary||||||Clayey polymict conglomerate, sandstone and sandy claystone.|
15977|Redbank Plains Formation|29720|6|Mentioned|p79|||||||||
15977|Redbank Plains Formation|30086|6|Mentioned|p4|||Tertiary age. Part of Booval Group.||||||
15977|Redbank Plains Formation|30087|4|Described|p3|||See also p4. Unit of Booval Group.||||||12-APR-07
15977|Redbank Plains Formation|30508|6|Mentioned|p87|||Tertiary. Redbank Plains Power Station site.||||||
15977|Redbank Plains Formation|30655|6|Mentioned|p28|||Refers Bryan and Jones (1946)||||||12-APR-07
15977|Redbank Plains Formation|31132|6|Mentioned|p150|||Refers Hill (1934)||||||
15977|Redbank Plains Formation|31333|6|Mentioned|p24|||Cainozoic fossils of stratigraphic significance or are illustrative of occurrence of a group in Cainozoic sediments.||||||
15977|Redbank Plains Formation|32178|6|Mentioned|p2|||Tertiary||||||
15977|Redbank Plains Formation|33381|4|Described|p121|||Tertiary. See also pp122,123. Of the Booval Group.||||||12-APR-07
15977|Redbank Plains Formation|34070|6|Mentioned|p3|||Tertiary||||||
15977|Redbank Plains Formation|34287|6|Mentioned|p202|||Eocene||||||
15977|Redbank Plains Formation|34354|6|Mentioned|p3|||Tertiary. See also p12.||||||12-APR-07
15977|Redbank Plains Formation|34505|6|Mentioned|p3|||See Fig.8. Of the Booval Group.||||||12-APR-07
15977|Redbank Plains Formation|36779|6|Mentioned|p8|||||||||
15977|Redbank Plains Formation|38074|5|Briefly described|Table 1|||||||||
15977|Redbank Plains Formation|38441|6|Mentioned|Map legend|Paleocene|Paleocene|||||||
15977|Redbank Plains Formation|39445|5|Briefly described|Table 14|||Clay deposits. See also p152.||||||12-APR-07
15977|Redbank Plains Formation|40247|6|Mentioned|p212|||||||||
15977|Redbank Plains Formation|40434|6|Mentioned|p29|||[Originally entered for Vic. CEBMar95]||||||
15977|Redbank Plains Formation|40623|5|Briefly described|p31|||||||||
15977|Redbank Plains Formation|41906|3|Fully described|Table 4 P33|||||||||
15977|Redbank Plains Formation|42336|4|Described|p6|||||||||
15977|Redbank Plains Formation|42541|5|Briefly described|p204|||||||||
15977|Redbank Plains Formation|43076|5|Briefly described|p22|||Middle Eocene age||||||
15977|Redbank Plains Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
15977|Redbank Plains Formation|43895|4|Described|p114,115|||Ceramic materials.||||||
15977|Redbank Plains Formation|43995|14|Not recorded|Tb.p10||Tertiary|||||||
15977|Redbank Plains Formation|44128|14|Not recorded|Tb.1,p426|||||||||
15977|Redbank Plains Formation|44510|14|Not recorded|p255,Fig.35||Tertiary|Obscures outcrop of Cooneana Formation.||||||
15977|Redbank Plains Formation|44581|2|Defined|p346-348,353|Oligocene|Eocene|Unconformably overlies Ipswich Coal Measures and Bundamba Group. (Late Eocene or Early Oligocene)||||||
15977|Redbank Plains Formation|44603|14|Not recorded|p130|||Included in Booval Group.||||||
15977|Redbank Plains Formation|44633|14|Not recorded|p7|||||||||
15977|Redbank Plains Formation|44687|6|Mentioned|p225|Oligocene|Eocene|Of Staines (1960). Equivalent of Darra Formation.||||||21-MAR-13
15977|Redbank Plains Formation|44734|14|Not recorded|p13|||Pine Mountain area. (?Eocene)||||||
15977|Redbank Plains Formation|44771|14|Not recorded|p3||Tertiary|Part of Booval Group.||||||
15977|Redbank Plains Formation|44772|14|Not recorded|p3|||||||||
15977|Redbank Plains Formation|44775|14|Not recorded|Map 2||Tertiary|||||||
15977|Redbank Plains Formation|44776|14|Not recorded|p4,fig.3|Oligocene|Eocene|Member of Booval Group.||||||12-APR-07
15977|Redbank Plains Formation|44781|14|Not recorded|p355|||||||||
15977|Redbank Plains Formation|44783|14|Not recorded|p2,11,12,19|||||||||
15977|Redbank Plains Formation|44810|14|Not recorded|p167 (Tb.)||Eocene|||||||
15977|Redbank Plains Formation|44885|14|Not recorded|p2,3, Fig.3|||||||||
15977|Redbank Plains Formation|60726|5|Briefly described|p2 Fig.1, p4, throughout text.  |Palaeocene|Palaeocene|Ipswich area, Booval Basin. ~70m thick. Highly diverse fossil fauna.|||||Mudstone, claystone, shale and fine sandstone. Fossiliferous.|
15977|Redbank Plains Formation|61155|5|Briefly described|p19|Early Eocene|Late Paleocene|Of the Booval Group.Overlain by Silkstone Formation. Age: ~58.5-55Ma. Thickness: ~67m. In the Brisbane region.||||||
15977|Redbank Plains Formation|68579|2|Defined|p221, 222|Oligocene|Eocene|Name introduced by Bryan and Jones (1950), after Redbank Plains Beds, Redbank Plains Series of Cameron (1907, 1923). Thickness: maximum 340ft, average 220 ft. Type area Redbank Plains. Includes fauna of fish, ostracods, insects and a lamellibranch; also angiosperm flora.||||Unconformably overlies Ipswich Coal Measures and Bundamba Group. Conformably overlain by Silkstone Formation.|Mudstones, clays and fissiles shales, variously coloured, often ferruginous; weathered parts include limonitic or haematitic nodules.|26-APR-13
15977|Redbank Plains Formation|69599|5|Briefly described|p586, p594|Eocene|Paleocene|Booval Basin. 67m thick. Fluvial to lacustrine sediments. Contains a diverse and rich fossil fauna and flora (listed).||Booval Group.||Is overlain conformably by Silkstone Formation. Is correlated with Darra Formation.|Claystone, sandstone and shale; surface exposures commonly comprise ferruginised mudstone nodules.|
16012|Reids Dome beds|13516|5|Briefly described|p145 fig 3, p143, p146-151|Early Permian|Early Permian|Denison Trough and western margin of Bowen Basin. Age APP2 - APP3.|||||Interbedded coal, sand, shale.|
16012|Reids Dome beds|22975|5|Briefly described|p34 Fig.6|Early Permian|Early Permian|||||||
16012|Reids Dome beds|22980|5|Briefly described|p249 Fig.2|Early Permian|Early Permian|||||||
16012|Reids Dome beds|23006|4|Described|p446|Permian|Permian|||||||
16012|Reids Dome beds|23060|5|Briefly described|15|||Geol Province: Bowen Basin||||||30-NOV-09
16012|Reids Dome beds|38198|6|Mentioned|p414|||||||||
16012|Reids Dome beds|38312|4|Described|p458|||||||||
16012|Reids Dome beds|38955|4|Described|p308|||||||||
16012|Reids Dome beds|39252|5|Briefly described|p13|||See also p16.||||||19-SEP-18
16012|Reids Dome beds|39253|6|Mentioned|p34|||||||||
16012|Reids Dome beds|39256|5|Briefly described|p53|||Floral types in coals||||||
16012|Reids Dome beds|39273|5|Briefly described|p305|||||||||
16012|Reids Dome beds|39412|6|Mentioned|p1|||||||||
16012|Reids Dome beds|39423|6|Mentioned|p49|||||||||
16012|Reids Dome beds|39494|6|Mentioned|p137|||||||||
16012|Reids Dome beds|39611|6|Mentioned|p256|||||||||
16012|Reids Dome beds|39815|6|Mentioned|p443|||||||||
16012|Reids Dome beds|39943|6|Mentioned|Table 5A|||||||||
16012|Reids Dome beds|39946|6|Mentioned|p212|||||||||
16012|Reids Dome beds|39994|4|Described|p200|||||||||
16012|Reids Dome beds|39999|5|Briefly described|p246|||||||||
16012|Reids Dome beds|40250|6|Mentioned|p34|||||||||
16012|Reids Dome beds|40539|6|Mentioned|p164|||||||||
16012|Reids Dome beds|41173|6|Mentioned|p91|||||||||
16012|Reids Dome beds|41225|6|Mentioned|p36|||||||||
16012|Reids Dome beds|41226|6|Mentioned|Table 1|||||||||
16012|Reids Dome beds|41246|6|Mentioned|Map legend|Permian||||||||
16012|Reids Dome beds|41247|6|Mentioned|p128|||||||||
16012|Reids Dome beds|41893|6|Mentioned|p514|||||||||
16012|Reids Dome beds|42249|6|Mentioned|p21|||||||||
16012|Reids Dome beds|42250|6|Mentioned|Fig.4 P31|||||||||
16012|Reids Dome beds|42254|6|Mentioned|p221|||||||||
16012|Reids Dome beds|42437|5|Briefly described|p820|||||||||
16012|Reids Dome beds|42648|5|Briefly described|p40|||||||||
16012|Reids Dome beds|42678|6|Mentioned|p257|||Bowen Basin||||||
16012|Reids Dome beds|42808|5|Briefly described|p156|||see also Fig.1 p157.||||||19-SEP-18
16012|Reids Dome beds|42856|5|Briefly described|Fig.2 P632|||||||||
16012|Reids Dome beds|42865|5|Briefly described|p18|||||||||
16012|Reids Dome beds|42911|6|Mentioned|p7|||||||||
16012|Reids Dome beds|43000|5|Briefly described|p107|||see also Fig.5,p112||||||
16012|Reids Dome beds|43017|5|Briefly described|Fig.3,p375|||||||||
16012|Reids Dome beds|43018|6|Mentioned|p388|||||||||
16012|Reids Dome beds|43029|5|Briefly described|p23|||||||||
16012|Reids Dome beds|43185|5|Briefly described|6-8||Early Permian|||||||
16012|Reids Dome beds|43204|5|Briefly described|Map Legend|Early Permian|Early Permian|||||underlies Aldebaran Sandstone||23-DEC-11
16012|Reids Dome beds|43213|5|Briefly described|p10, p152, p239|Permian|Permian|Mollan et al. (1969). Bowen Basin. Fluvial to deltaic deposits in a graben and half-graben structure. Contains abundant Glossopteris flora.||||Overlies Fork Lagoons beds. Is overlain conformably by Tiverton Formation.|Basal conglomeratic sandstone overlain by black to dark grey siltstone, mudstone and minor fine sandstone and limestone; above which are sandstone, siltstone, conglomerate and coal seams.|
16012|Reids Dome beds|43483|6|Mentioned|14||Permian|||||||
16012|Reids Dome beds|46989|6|Mentioned|p216|||||||||
16012|Reids Dome beds|60294|5|Briefly described|p123|||Includes carbonaceous shales. Geological Province: Denison Trough, Bowen Basin.||||||
16012|Reids Dome beds|60386|6|Mentioned|p296|Artinskian||Bowen/Sydney Basin. Non-marine.||||||
16012|Reids Dome beds|61377|6|Mentioned|p156 Tb. SU2|Early Permian|Early Permian|A reservoir unit in Queensland.||||||07-FEB-11
16012|Reids Dome beds|62357|5|Briefly described|p524 Fig. 7, p529 Fig.13|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||
16012|Reids Dome beds|63172|6|Mentioned|p301, p305|Early Permian|Early Permian|A Queensland unit.||||||07-FEB-11
16012|Reids Dome beds|64665|5|Briefly described|p52, p53 Fig.2.|Early Permian|Early Permian|Denison Trough, Bowen Basin. A fluvio-deltaic succession deposited in a half-graben system.||||||
16012|Reids Dome beds|64856|5|Briefly described|p43, p46, p50||Sakmarian|Denison Trough. Oldest palynofloras in this unit assigned to APP2 (285-293 Ma using AGSO 1996 definition, which corresponds to Sakmarian). Correlated with Arbroath beds.|| ||||29-NOV-17
16012|Reids Dome beds|64857|6|Mentioned|p113 Fig.3|||Bowen Basin.||||||
16012|Reids Dome beds|65112|5|Briefly described|p313; Fig 4 p314|Early Permian|Early Permian|Non-marine sedimentary infill observed in the Denison Trough, bounded by half grabens. Up to 4000m. Fill probablly  derived from silicic and/or basaltic volcanism.||||Overlain by Cattle Creek Formation.||22-MAR-12
16012|Reids Dome beds|65113|5|Briefly described|p343, 345,Fig 4 p340, Fig 6 p344|Sakmarian|Sakmarian|Deposited as a series of non-volcanic half grabens, in the Denison Trough. Syn-rift deposition. Underlies the Cattle Creek Formation. Forms upper part of Supersequence A.||||||
16012|Reids Dome beds|65114|5|Briefly described|p383 Tb.1, p385 Fig.3, p388|Sakmarian||285-280 Ma; Tectonic unit: Bowen Basin - Denison Trough and related western sub-basins; part of Supersequence A.||||||19-SEP-18
16012|Reids Dome beds|65115|6|Mentioned|p407, Fig 2 p403|Permian|Permian|Underlies the Cattle Creek Formation in the Denison Trough, Bowen Basin.||||||14-NOV-12
16012|Reids Dome beds|65116|5|Briefly described|p437, Fig 2 p436|Early Permian|Early Permian|Underlies the Cattle Creek Formation in the Denison Trough, Bowen Basin. Equivalent lacustrine and fluvial sediments are interbedded with the Boggabri Volcanics in the Gunnedah Basin.||||||
16012|Reids Dome beds|65118|5|Briefly described|Fig 2 p479|Permian|Permian|Underlies the Cattle Creek Formation in the Denison Trough in the Bowen Basin.||||||
16012|Reids Dome beds|65119|6|Mentioned|Fig 14 p521|||Present in the MacIntyre 1 well.||||||
16012|Reids Dome beds|66188|6|Mentioned|443, fig 17|Early Permian|Early Permian|Bowen Basin||||||
16012|Reids Dome beds|66615|6|Mentioned|p2 Fig.1, p8|Early Permian|Early Permian|Denison Trough, Bowen Basin.||||||
16012|Reids Dome beds|67402|4|Described|p21, p64, p65|Artinskian|Sakmarian|Bowen Basin. Approximately 400m thick.Deposited in fluvial, alluvial, lacustrine or marginal marine environments. See also p66 fig BWW4, p72, p73, p265.||||Overlain by the Cattle Creek Formation.|Sandstone, mudstone, coal and some conglomerate.|
16012|Reids Dome beds|68411|5|Briefly described|Map Legend|Permian|Permian|Galilee Basin||Of the Back Creek Group.||Conformably overlain by the Colinlea Sandstone. Unconformably underlain by the Joe Joe Group.|Siltstone, shale, labile sandstone, lithic conglomerate and coal.|
16012|Reids Dome beds|68576|5|Briefly described|Q_4: p3, p10, p19|Cisuralian|Cisuralian|Denison Trough and western Bowen Basin. Appears as Reid's Dome Beds on p10 and p19. Contains abundant Glossopteris/Gangamopteris flora and rare marine fossils.||||Is overlain by Sirius Mudstone Member (Cattle Creek Formation).|Variable lithologies: carbonaceous sandstone, grey siltstone, shale and coal above thick dark shale with anhydrite, dolomite, coal, sandstone and siltstone. Thick volcanolithic pebble conglomerate and volcanolithic sandstone locally.|
16012|Reids Dome beds|68679|5|Briefly described|p373 Fig.5.67, p378-379, p381, p383-384|Permian|Permian|See also p469. Power (1967). Denison Trough, Bowen Basin. >2800m thick. Alluvial fan, alluvial plain, lake deposits in half-grabens. Properties of the coal are described in some detail. Produces gas and minor condensate.||||Overlies Combarngo Volcanics. Is overlain by Back Creek Group and Cattle Creek Formation (and interfingers with the latter).|Quartzose to sublabile sandstone, mudstone, siltstone, conglomerate, coal.|
16012|Reids Dome beds|68731|6|Mentioned|p201 Fig 3.110|Cisuralian|Cisuralian|Bowen Basin.||||||
16012|Reids Dome beds|70815|6|Mentioned|p3-4, 8|||Bowen Basin. Also appears variously as Reid's Dome beds, Reid's Dome Beds and even Reid's Domes beds. Locally over 2700m thick. Vitrinite reflectance values (for top 300m) mapped.||||||
16012|Reids Dome beds|70856|5|Briefly described|Map Legend|Permian|Permian|||Back Creek Group.||Overlain by Cattle Creek Formation.|Siltstone, shale, labile sandstone, lithic conglomerate and coal.|
16012|Reids Dome beds|71265|5|Briefly described|p589|Cisuralian|Cisuralian|Bowen Basin.||||Is overlain by Cattle Creek Formation.||
16012|Reids Dome beds|71701|5|Briefly described|p155, p170|Kungurian|Artinskian|Denison Trough, Bowen Basin.||||Unconformably overlain by the Sirius Mudstone Member of the Cattle Creek Formation.||
16012|Reids Dome beds|71710|6|Mentioned|p368|||southern Bowen Basin.||||Age-equivalent correlation to Carmila beds (Bowen Basin); palynologically correlatable to Aramac Coal Measures (northern Galilee Basin)||
16012|Reids Dome beds|72088|5|Briefly described|p8, p46, p91|Kungurian|Asselian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Faulted against the Cattle Creek Formation. Unconformably overlain by the Sirius Mudstone Member.||
16012|Reids Dome beds|72297|5|Briefly described|p694, p704-705, p745|Permian|Permian|Bowen Basin. Variable thickness and lithology. Coal properties briefly described; indicative properties of export PCI and thermal coals tabulated. Oil and gas source rock; reservoirs in upper parts.||||||
16012|Reids Dome beds|73472|6|Mentioned|p115|Artinskian|Sakmarian|||||Overlain by Sirius Mudstone Member (Cattle Creek Formation). Equivalent to Cattle Creek Formation.||
16013|Reids Dome coal|39275|6|Mentioned|p332|||||||||
16052|Rewan Formation|22464|5|Briefly described|p9|Middle Triassic|Early Triassic|Cooper Basin||||||
16052|Rewan Formation|22757|4|Described|Table4,p9||Early Triassic|840 m thick. Unconformable on Blackwater Group. Unconformably overlain by Clematis Sandstone||||||
16052|Rewan Formation|23003|5|Briefly described|p423 Table 1|Triassic|Triassic|||||||
16052|Rewan Formation|23004|5|Briefly described|p431 Table 1|Triassic|Triassic|||||||
16052|Rewan Formation|23037|6|Mentioned|Fig 3|Triassic|Late Permian|Overlying unit Back Creek Group.||||||
16052|Rewan Formation|23425|6|Mentioned|p391.|||||||||
16052|Rewan Formation|23769|4|Described|p862|Early Triassic|Early Triassic|Parent: Mimosa Group.  Geological Province: Bowen Basin.||||||
16052|Rewan Formation|23883|5|Briefly described|p129 Fig. 11.2|Triassic|Triassic|Geological Province: Great Australian Superbasin.||||||
16052|Rewan Formation|23982|5|Briefly described|p35 Fig.7|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
16052|Rewan Formation|24069|5|Briefly described|p284|Early Triassic|Early Triassic|Geological Province: Surat Basin.||||||
16052|Rewan Formation|24071|5|Briefly described|p319|Triassic|Triassic|Geological Province: Galilee Basin.||||||
16052|Rewan Formation|24077|5|Briefly described|p410 Tb. 2|Middle Triassic|Early Triassic|Of Mimosa Group.  Max. thickness: 615m.  Geological Province: Bowen Basin.See also p411 Tb.3.||||||
16052|Rewan Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16052|Rewan Formation|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||17-MAR-05
16052|Rewan Formation|24615|5|Briefly described|CD|Triassic|Triassic|[Rr].  Green lithic sandstone, green and red mudstone and sandstone.||||||
16052|Rewan Formation|29385|6|Mentioned|p81|||Lower Triassic.||||||
16052|Rewan Formation|29387|6|Mentioned|Table 3|||See also Table 4. Triassic.||||||
16052|Rewan Formation|29388|6|Mentioned|p62|||Stratigraphy.||||||
16052|Rewan Formation|29389|6|Mentioned|p18|||Early Triassic.||||||
16052|Rewan Formation|29390|6|Mentioned|p54|||Only oil discovery in Bowen Basin.||||||
16052|Rewan Formation|29391|6|Mentioned|Table 3|||Appears on P18, see also Table 4 on P19.||||||
16052|Rewan Formation|29393|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|29409|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|29410|6|Mentioned|p273|||Correlation diagram P275. Conformably overlies Bandanna Fm.||||||
16052|Rewan Formation|29411|5|Briefly described|p201|||||||||
16052|Rewan Formation|29412|4|Described|p208|||Appears throughout article.||||||
16052|Rewan Formation|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
16052|Rewan Formation|29721|6|Mentioned|Table 65|||||||||
16052|Rewan Formation|30102|4|Described|p9|||See also P10-13. Lower Triassic age.||||||
16052|Rewan Formation|30103|6|Mentioned|p8|||||||||
16052|Rewan Formation|30137|6|Mentioned|p2|||Triassic age||||||
16052|Rewan Formation|30140|6|Mentioned|p2|||Triassic age. Lithology||||||
16052|Rewan Formation|30141|6|Mentioned|p135|||||||||
16052|Rewan Formation|30351|6|Mentioned|Fig.4|||Fig.4 on P32||||||
16052|Rewan Formation|30451|4|Described|p66|||Lower Triassic age||||||
16052|Rewan Formation|30455|5|Briefly described|p1|||See also P2-3. Triassic age||||||
16052|Rewan Formation|30457|6|Mentioned|p96|||||||||
16052|Rewan Formation|30458|6|Mentioned|p3|||Triassic age||||||
16052|Rewan Formation|30459|6|Mentioned|p309|||||||||
16052|Rewan Formation|30460|6|Mentioned|p1|||Triassic age. See also P3-22,24-27, Fig.1,2||||||
16052|Rewan Formation|30461|6|Mentioned|p100|||||||||
16052|Rewan Formation|30465|6|Mentioned|p4|||||||||
16052|Rewan Formation|30466|6|Mentioned|p4|||Triassic age||||||
16052|Rewan Formation|30468|6|Mentioned|p385|||||||||
16052|Rewan Formation|30472|6|Mentioned|p134|||Pollen distribution||||||
16052|Rewan Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
16052|Rewan Formation|30545|6|Mentioned|p22|||Triassic||||||
16052|Rewan Formation|30546|6|Mentioned|p107|||Correlation.Lower Triassic age.||||||
16052|Rewan Formation|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
16052|Rewan Formation|30549|6|Mentioned|p26|||||||||
16052|Rewan Formation|30565|6|Mentioned|p120|||||||||
16052|Rewan Formation|30691|4|Described|p14|||See also Table 4,6. Lower Triassic age||||||
16052|Rewan Formation|30696|4|Described|Table 3|||Lower Triassic age||||||
16052|Rewan Formation|30698|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|30699|6|Mentioned|p53|||Stratigraphy||||||
16052|Rewan Formation|30701|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|30743|6|Mentioned|p24|||Geological map||||||
16052|Rewan Formation|30851|6|Mentioned|p366.|||||||||
16052|Rewan Formation|30852|4|Described|Fig.2|||||||||
16052|Rewan Formation|30853|6|Mentioned|p9|||||||||
16052|Rewan Formation|30915|6|Mentioned|p98|||||||||
16052|Rewan Formation|30916|6|Mentioned|p98|||On table||||||
16052|Rewan Formation|31084|6|Mentioned|p13|||L. Triassic||||||
16052|Rewan Formation|31115|5|Briefly described|p32|||See also P33-34. Triassic||||||
16052|Rewan Formation|31116|4|Described|p11|||See also P1. Triassic||||||
16052|Rewan Formation|31120|6|Mentioned|Fig. 2|||||||||
16052|Rewan Formation|31121|6|Mentioned|p388|||||||||
16052|Rewan Formation|31122|6|Mentioned|p344|||||||||
16052|Rewan Formation|31145|6|Mentioned|p7|||||||||
16052|Rewan Formation|31167|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|31260|6|Mentioned|p16|||Facies analysis||||||
16052|Rewan Formation|31303|4|Described|Table 1|||||||||
16052|Rewan Formation|31305|4|Described|p571|||Mention Table 1||||||
16052|Rewan Formation|31369|4|Described|p26|||See also P27. Triassic||||||
16052|Rewan Formation|31398|6|Mentioned|p268|||L.Triassic. Fauna||||||
16052|Rewan Formation|31401|6|Mentioned|p33|||On Table 3.||||||
16052|Rewan Formation|31531|6|Mentioned|p13|||||||||
16052|Rewan Formation|31553|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|31620|5|Briefly described|p87|||See also P88-89||||||
16052|Rewan Formation|31647|6|Mentioned|Fig. 9|||||||||
16052|Rewan Formation|31656|4|Described|Table 2|||Triassic (Mimosa Gp.)||||||
16052|Rewan Formation|31690|6|Mentioned|p35|||||||||
16052|Rewan Formation|31979|6|Mentioned|p10|||||||||
16052|Rewan Formation|31984|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32040|6|Mentioned|p885|||Stratigraphic sequence||||||
16052|Rewan Formation|32136|6|Mentioned|p2|||Triassic. Geol map near Munduberra No.1||||||
16052|Rewan Formation|32138|6|Mentioned|p396|||||||||
16052|Rewan Formation|32139|6|Mentioned|p579|||||||||
16052|Rewan Formation|32177|6|Mentioned|p145|||||||||
16052|Rewan Formation|32193|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|32490|4|Described|Table 1|||L.Triassic||||||
16052|Rewan Formation|32493|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32496|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32553|4|Described|p40|||||||||
16052|Rewan Formation|32556|4|Described|Table 4|||Triassic||||||
16052|Rewan Formation|32577|4|Described|p25|||Perm.-L.Triass.||||||
16052|Rewan Formation|32578|6|Mentioned|p347|||Perm. Strat. table||||||
16052|Rewan Formation|32689|6|Mentioned|Fig.2|||Strat. correlation table||||||
16052|Rewan Formation|32797|6|Mentioned|p10|||||||||
16052|Rewan Formation|32840|6|Mentioned|p1|||See also P26||||||
16052|Rewan Formation|32944|6|Mentioned|p703|||L.Triassic||||||
16052|Rewan Formation|33059|4|Described|Table 1|||L.Trias.||||||
16052|Rewan Formation|33078|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33079|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33086|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33092|5|Briefly described|p6|||Strat. table||||||
16052|Rewan Formation|33096|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33128|5|Briefly described|p51|||Geochemistry||||||
16052|Rewan Formation|33250|6|Mentioned|p140|||||||||
16052|Rewan Formation|33251|6|Mentioned|p2|||||||||
16052|Rewan Formation|33363|5|Briefly described|p115|||Triassic.||||||
16052|Rewan Formation|33366|6|Mentioned|Fig.3|||Triassic.||||||
16052|Rewan Formation|33368|6|Mentioned|p12|||Consuelo N.S.3 log.||||||
16052|Rewan Formation|33369|6|Mentioned|p214|||Strat. succession in GSQ Jericho 1.||||||
16052|Rewan Formation|33372|4|Described|p21|||Mention P16. Q.D.M. Aramac 1 & Hexham 1.||||||
16052|Rewan Formation|33390|5|Briefly described|p6|||||||||
16052|Rewan Formation|33451|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33530|5|Briefly described|Table 1|||Triassic||||||
16052|Rewan Formation|33561|6|Mentioned|p102|||||||||
16052|Rewan Formation|33639|5|Briefly described|p10|||L.Triass.||||||
16052|Rewan Formation|33640|4|Described|Table 3|||Triassic.||||||
16052|Rewan Formation|33646|5|Briefly described|p11|||||||||
16052|Rewan Formation|33647|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33648|6|Mentioned|p18|||Strat.||||||
16052|Rewan Formation|33674|4|Described|p412|||||||||
16052|Rewan Formation|33675|4|Described|p412|||||||||
16052|Rewan Formation|33774|3|Fully described|p39|||||||||
16052|Rewan Formation|34009|6|Mentioned|Table III|||||||||
16052|Rewan Formation|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
16052|Rewan Formation|34061|6|Mentioned|p53|||||||||
16052|Rewan Formation|34094|6|Mentioned|p1-4,Figs.2,3,4||Triassic|||||||
16052|Rewan Formation|34095|6|Mentioned|p3,4,6,Figs.5,6||Triassic|||||||
16052|Rewan Formation|34133|6|Mentioned|p2|||See also PP28,29||||||
16052|Rewan Formation|34172|6|Mentioned|p52|||||||||
16052|Rewan Formation|34174|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|34212|6|Mentioned|p2|||See also PP6,14 etc. Jurassic.||||||
16052|Rewan Formation|34218|6|Mentioned|p9|||Triassic||||||
16052|Rewan Formation|34235|6|Mentioned|p92|||||||||
16052|Rewan Formation|34254|6|Mentioned|Table 7.1|||||||||
16052|Rewan Formation|34276|6|Mentioned|p42|||Triassic||||||
16052|Rewan Formation|34314|5|Briefly described|Table 3|||Triassic. Mimosa Group||||||
16052|Rewan Formation|34331|6|Mentioned|p458|||L.Triassic||||||
16052|Rewan Formation|34391|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|34543|6|Mentioned|p98|||||||||
16052|Rewan Formation|34574|6|Mentioned|p115|||||||||
16052|Rewan Formation|34613|4|Described|Table 3|||||||||
16052|Rewan Formation|34614|6|Mentioned|p29|||||||||
16052|Rewan Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
16052|Rewan Formation|35079|6|Mentioned|p424|||||||||
16052|Rewan Formation|35095|6|Mentioned|p115|||||||||
16052|Rewan Formation|35148|4|Described|p414|||See also Table 1.||||||
16052|Rewan Formation|35280|6|Mentioned|p143|||||||||
16052|Rewan Formation|35426|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|35428|6|Mentioned|p125|||Biostratigraphy||||||
16052|Rewan Formation|35435|6|Mentioned|p44|||Summarised stratigraphic table of the Artesian Basin.||||||
16052|Rewan Formation|35457|6|Mentioned|p633|||Also Fig.4 biostratigraphic relationships||||||
16052|Rewan Formation|35467|6|Mentioned|p178|||||||||
16052|Rewan Formation|35488|6|Mentioned|p87|||||||||
16052|Rewan Formation|35560|6|Mentioned|p292|||||||||
16052|Rewan Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
16052|Rewan Formation|35621|6|Mentioned|p331|||||||||
16052|Rewan Formation|35822|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|35859|6|Mentioned|p225|||||||||
16052|Rewan Formation|35873|4|Described|p16|||||||||
16052|Rewan Formation|36121|6|Mentioned|p25|||||||||
16052|Rewan Formation|36241|6|Mentioned|p110|||||||||
16052|Rewan Formation|36243|6|Mentioned|p74|||See also Table 3A.||||||
16052|Rewan Formation|36333|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|36825|6|Mentioned|p21|||||||||
16052|Rewan Formation|36899|6|Mentioned|p1085|||See also P1092.||||||
16052|Rewan Formation|36914|6|Mentioned|p87|||||||||
16052|Rewan Formation|36921|6|Mentioned|p175|||See also Table 1.||||||
16052|Rewan Formation|36925|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|37070|5|Briefly described|p70|||||||||
16052|Rewan Formation|37072|5|Briefly described|p90|||||||||
16052|Rewan Formation|37074|3|Fully described|p105|||||||||
16052|Rewan Formation|37075|5|Briefly described|Table 1|||||||||
16052|Rewan Formation|37076|4|Described|p121|||||||||
16052|Rewan Formation|37077|6|Mentioned|p130|||||||||
16052|Rewan Formation|37078|5|Briefly described|p135|||||||||
16052|Rewan Formation|37079|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|37080|5|Briefly described|p150|||||||||
16052|Rewan Formation|37262|6|Mentioned|p285|||||||||
16052|Rewan Formation|37288|6|Mentioned|p41|||||||||
16052|Rewan Formation|37400|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|37451|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|37610|6|Mentioned|p302|||||||||
16052|Rewan Formation|37749|6|Mentioned|p186|||||||||
16052|Rewan Formation|37812|6|Mentioned|p656|||||||||
16052|Rewan Formation|37858|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|37859|6|Mentioned|Table 1|||See also Tables 2 & 3.||||||
16052|Rewan Formation|38153|6|Mentioned|p373|||||||||
16052|Rewan Formation|38358|6|Mentioned|p13|||||||||
16052|Rewan Formation|38375|6|Mentioned|p545|||||||||
16052|Rewan Formation|38447|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|38713|6|Mentioned|p330|||Now named Arcadia Formation.||||||
16052|Rewan Formation|39217|6|Mentioned|p49|||Refers Evans(1966)||||||
16052|Rewan Formation|39219|6|Mentioned|p46|||Microflora||||||
16052|Rewan Formation|39252|6|Mentioned|p26|||||||||
16052|Rewan Formation|39260|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|39261|6|Mentioned|Fig. 9|||||||||
16052|Rewan Formation|39264|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|39270|5|Briefly described|p282|||||||||
16052|Rewan Formation|39275|6|Mentioned|p332|||||||||
16052|Rewan Formation|39412|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|39445|5|Briefly described|Table 9|||||||||
16052|Rewan Formation|39478|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|39491|4|Described|p18|||||||||
16052|Rewan Formation|39813|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|40095|6|Mentioned|Fig.6|||||||||
16052|Rewan Formation|40123|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|40249|6|Mentioned|p41|||Mention Fig.2||||||
16052|Rewan Formation|40634|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|40767|6|Mentioned|p18|||||||||
16052|Rewan Formation|40999|6|Mentioned|p298|||||||||
16052|Rewan Formation|41034|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|41116|4|Described|p433|||||||||
16052|Rewan Formation|41159|4|Described|p341|||||||||
16052|Rewan Formation|41198|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|41210|6|Mentioned|p165|||||||||
16052|Rewan Formation|41216|6|Mentioned|p304|||||||||
16052|Rewan Formation|41266|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|41330|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|41475|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|41535|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|41707|6|Mentioned|Fig.8|||||||||
16052|Rewan Formation|41710|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|41725|6|Mentioned|p399|||See also Fig.2||||||
16052|Rewan Formation|42249|6|Mentioned|p23|||||||||
16052|Rewan Formation|42250|6|Mentioned|Fig.3 P30|||||||||
16052|Rewan Formation|42446|4|Described|p10|||||||||
16052|Rewan Formation|42447|6|Mentioned|Fig. 2|||||||||
16052|Rewan Formation|42463|6|Mentioned|Fig.5 P172|||||||||
16052|Rewan Formation|42492|5|Briefly described|Table 2 P14|||||||||
16052|Rewan Formation|42713|5|Briefly described|Fig. P18|||||||||
16052|Rewan Formation|42932|5|Briefly described|Fig.21|||||||||
16052|Rewan Formation|43017|5|Briefly described|p379|||||||||
16052|Rewan Formation|43072|6|Mentioned|p31|||||||||
16052|Rewan Formation|43812|6|Mentioned|Fig.3,p145|||||||||
16052|Rewan Formation|43851|14|Not recorded|Tb p106,113||Early Triassic|||||||
16052|Rewan Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
16052|Rewan Formation|43912|14|Not recorded|p2|||(Sunnybank No.1)||||||
16052|Rewan Formation|43920|14|Not recorded|p74|||||||||
16052|Rewan Formation|43922|14|Not recorded|p326|||L.Triassic, Bowen Basin.||||||
16052|Rewan Formation|43923|6|Mentioned|p1||Triassic|||||||
16052|Rewan Formation|43977|14|Not recorded|p576|||||||||
16052|Rewan Formation|43982|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|43987|14|Not recorded|p265-6,269-271,275,|||p277-279||||||
16052|Rewan Formation|43988|14|Not recorded|Map Legend||Triassic|Of Mimosa Group||||||
16052|Rewan Formation|43989|14|Not recorded|Map Legend||Early Triassic|||||||
16052|Rewan Formation|43990|14|Not recorded|Map Legend||Triassic|Part of Mimosa Group.||||||
16052|Rewan Formation|43994|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|43995|14|Not recorded|Tb.p9,23,53,Fig.14|Permian|Carboniferous|||||||
16052|Rewan Formation|43996|14|Not recorded|p88|||||||||
16052|Rewan Formation|43997|14|Not recorded|p113|||||||||
16052|Rewan Formation|43998|4|Described|p12,13,17,map||Triassic|||||||
16052|Rewan Formation|44000|14|Not recorded|p40|||||||||
16052|Rewan Formation|44003|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|44020|14|Not recorded|p10|||||||||
16052|Rewan Formation|44022|14|Not recorded|Map Legend||Triassic|||||||
16052|Rewan Formation|44023|4|Described|Tb.3||Triassic|||||||
16052|Rewan Formation|44031|14|Not recorded|p6||Triassic|||||||
16052|Rewan Formation|44040|14|Not recorded|p14|||||||||
16052|Rewan Formation|44085|2|Defined|Opp.4,12,13,15|||||||||
16052|Rewan Formation|44091|14|Not recorded|p53,54||Triassic|||||||
16052|Rewan Formation|44095|14|Not recorded|p284|||||||||
16052|Rewan Formation|44096|2|Defined|Fig.26,p187-8,193|||Overlies Bandanna Formation.||||||
16052|Rewan Formation|44115|14|Not recorded|p18,19,21|||||||||
16052|Rewan Formation|44118|14|Not recorded|Map Legend||Triassic|||||||
16052|Rewan Formation|44124|14|Not recorded|p1,2,4,5,10,12|||||||||
16052|Rewan Formation|44129|14|Not recorded|p95-96||Triassic|||||||
16052|Rewan Formation|44130|14|Not recorded|p280|||Unconformably overlain by Clematis Sandstone.||||||
16052|Rewan Formation|44166|14|Not recorded|p1|||||||||
16052|Rewan Formation|44169|2|Defined|Tb.1,6,8,9,map|||||||||
16052|Rewan Formation|44170|2|Defined|p1,6,12-17,19,25,28,||Early Triassic|p30,31,35-38,53-56,Tb.1,Pl.1,map||||||
16052|Rewan Formation|44172|14|Not recorded|Tb.1,p1325,1339||Triassic|Ref. to Hill 1957.||||||
16052|Rewan Formation|44218|14|Not recorded|p18|||||||||
16052|Rewan Formation|44242|14|Not recorded|p14|||||||||
16052|Rewan Formation|44243|14|Not recorded|p649,map,650||Triassic|||||||
16052|Rewan Formation|44337|5|Briefly described|Map Legend||Triassic|Lithology.||||||
16052|Rewan Formation|44381|14|Not recorded|p7|||||||||
16052|Rewan Formation|44390|14|Not recorded|p6,8,13,14,Tb.1,||Early Triassic|Of Mimosa Group.||||||
16052|Rewan Formation|44391|14|Not recorded|Map Legend||Early Triassic|||||||
16052|Rewan Formation|44419|14|Not recorded|p274|||||||||
16052|Rewan Formation|44420|14|Not recorded|p1-3,6-11,15,22,28||Early Triassic|||||||
16052|Rewan Formation|44421|14|Not recorded|p6,8-11,18||Triassic|||||||
16052|Rewan Formation|44422|14|Not recorded|p150,152,153||Early Triassic|||||||
16052|Rewan Formation|44426|14|Not recorded|p11-12||Triassic|Dicroidium; Triassic from micro and macrofaunas. "A correlation between the Rewan Formation and Narrabeen Group of the Sydney Basin is indicated."||||||
16052|Rewan Formation|44577|14|Not recorded|p137|||||||||
16052|Rewan Formation|44607|14|Not recorded|p10|||||||||
16052|Rewan Formation|44609|14|Not recorded|p64|||||||||
16052|Rewan Formation|44610|14|Not recorded|p47-49|||||||||
16052|Rewan Formation|44618|14|Not recorded|p511-513||Triassic|||||||
16052|Rewan Formation|44640|14|Not recorded|p36,map|||||||||
16052|Rewan Formation|44651|14|Not recorded|p117|||||||||
16052|Rewan Formation|44652|14|Not recorded|p70,73,74||Triassic|||||||
16052|Rewan Formation|44668|14|Not recorded|p59|||||||||
16052|Rewan Formation|44697|14|Not recorded|p91|||||||||
16052|Rewan Formation|44721|14|Not recorded|p28-36||Triassic|||||||
16052|Rewan Formation|44746|14|Not recorded|p50|||||||||
16052|Rewan Formation|44787|14|Not recorded|p121,Tb.p123,124,127||Early Triassic|||||||
16052|Rewan Formation|44792|14|Not recorded|p15|||||||||
16052|Rewan Formation|44815|14|Not recorded|unknown (p313-346)|Triassic|Permian|||||||
16052|Rewan Formation|45031|14|Not recorded|Fig.3,||Triassic|||||||
16052|Rewan Formation|45071|3|Fully described|p70|||See also Table 14||||||
16052|Rewan Formation|45073|6|Mentioned|p59|||Correlation chart||||||
16052|Rewan Formation|45095|6|Mentioned|p18|||Refers Malone et al. (1969)||||||
16052|Rewan Formation|45151|6|Mentioned|p15|||||||||
16052|Rewan Formation|46849|6|Mentioned|p194|||||||||
16052|Rewan Formation|46881|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
16052|Rewan Formation|46949|6|Mentioned|p96|||||||||
16052|Rewan Formation|48600|14|Not recorded|p13,20|||Shelf sediments. Springsure area.||||||
16052|Rewan Formation|48606|14|Not recorded|p14|||(H/55-8).||||||
16052|Rewan Formation|48626|14|Not recorded|p1,3,23-26,51,55,||Triassic|Pl.1,Fig.1,2.||||||
16052|Rewan Formation|48898|4|Described|p56|||Triassic. See also PP55,58 etc||||||
16052|Rewan Formation|48900|2|Defined|p41|Triassic|Triassic|||||||
16052|Rewan Formation|48915|6|Mentioned|Table 1|||Triassic. See also P10||||||
16052|Rewan Formation|48919|4|Described|p29|||L.Triassic. See also P30-32||||||
16052|Rewan Formation|48920|3|Fully described|p30|||Triassic||||||
16052|Rewan Formation|48922|4|Described|p22|||||||||
16052|Rewan Formation|48947|6|Mentioned|p10|||||||||
16052|Rewan Formation|48951|6|Mentioned|Table|||||||||
16052|Rewan Formation|48995|6|Mentioned|p128|||See also Fig.3.||||||
16052|Rewan Formation|49010|6|Mentioned|Fig.4|||Galilee Basin||||||
16052|Rewan Formation|49011|6|Mentioned|Fig.3|||Galilee Basin||||||
16052|Rewan Formation|49644|5|Briefly described|Table|||||||||
16052|Rewan Formation|50215|5|Briefly described|Map Legend|Triassic|Triassic|Green and reddish brown mudstone, lithic sandstone and minor conglomerate.||||||18-JUN-09
16052|Rewan Formation|50273|5|Briefly described|Map legend|Triassic|Triassic|Lithic sandstone and green to reddish brown mudstone and minor conglomerate.||||||
16052|Rewan Formation|50602|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Green lithic sandstone, mudstone.||||||
16052|Rewan Formation|60700|5|Briefly described|p37|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16052|Rewan Formation|61772|6|Mentioned|p131|||||||||
16052|Rewan Formation|61832|5|Briefly described|p187|Early Triassic|Early Triassic|Sandstone and fine-grained rocks. Geological Province: Bowen Basin.||||||05-OCT-06
16052|Rewan Formation|62921|5|Briefly described|p877-879, p881-883|Early Triassic|Changhsingian|Not subdivided in the Galilee Basin (Exon, 1970). In the Bowen Basin it was elevated to Group status by Jensen (1975) who divided it into two Formations (Arcadia Formation and Sagittarius Sandstone). Contains Late Permian and Early Triassic miospores. This article describes the first tetrapod (Lydekkerina huxleyi) from this Formation, the second lydekkerinid from Australia. This Formation is equivalent in age to the Lystrosaurus Assemblage Zone in South Africa.||||Unconformably overlies Bandanna Formation. Is overlain by Dunda Beds. Correlated with Rewan Group (Bowen Basin). Said to conformably overlie Betts Creek Beds (Blackwater Group).|Pale buff to yellow, fine-grained sandstones and mudstones.|
16052|Rewan Formation|63172|6|Mentioned|p21|||Geological Province: Bowen Basin. Mentioned in the context of the combined units - "Rewan Formation-Clematis Sandstone interval".||||||07-FEB-11
16052|Rewan Formation|64665|6|Mentioned|p54.|Triassic|Triassic|Red-bed deposits.||||||
16052|Rewan Formation|64856|5|Briefly described|p68, p72|||Name used 1950s to 1970s. Superseded by Rewan Group.|| ||||29-NOV-17
16052|Rewan Formation|65003|5|Briefly described|p6|||Of Bowen Basin. Unconformably overlies the coal measures [?Baralaba Coal Measures].||||Overlain by the Clematis Group and Moolayember Formation.||30-MAR-12
16052|Rewan Formation|65388|6|Mentioned|p159, 202|||Bowen Basin, Galilee Basin. Replaced by Rewan Group by Jensen in 1975.||||||
16052|Rewan Formation|65489|5|Briefly described|p144 Fig.53|Early Triassic|Early Triassic|Koburra Trough, Galilee Basin.||||Overlies Betts Creek Beds. Is overlain by Dunda Formation.||
16052|Rewan Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. Also appears as Rewan Fm/Gp in Fig.5.||||||
16052|Rewan Formation|67133|5|Briefly described|p9|||Primarily fluvial and lacustrine environments. Two samples of this unit were analysed by XRD and optical microscopy for this study; one was smectite-rich while the other was illite-rich.||Rewan Group.|||Includes sandstones which are generally quartzose, partly lithic (volcanic fragments) and with a clayey matrix.|
16052|Rewan Formation|67323|5|Briefly described|p84|Triassic|Triassic|Eastern Galilee Basin.||||Tentatively correlated with Warang Sandstone.||
16052|Rewan Formation|67402|5|Briefly described|p43 tbl HPB1, p52, p65|Olenekian|Changhsingian|Galilee Basin. Prospective reservoir unit for the storage of carbon dioxide; together with the Clematis Sandstone may be able to store 982 Megatonnes of carbon dioxide. More than 100m thick. See also  p69, p124 fig GLL1, p125 tbl GLL1, p128 fig GLL8, p129 fig GLL9, p131 fig GLL12, p132-p137, p140, p142, p144, p265, p300, p305.||||Overlies the Betts Creek beds.|Interbedded mudstone, siltstone and sandstone.|
16052|Rewan Formation|67669|5|Briefly described|p11|Early Triassic|Early Triassic|Of Bowen Basin.||Unit of Rewan Group.||||
16052|Rewan Formation|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Unconformably underlain by the Blackwater Group. Conformably overlain by the Clematis Group.|Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanolithic pebble conglomerate (at base).|
16052|Rewan Formation|68413|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably overlain by the Warang Sandstone.|Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanolithic pebble conglomerate (at base).|
16052|Rewan Formation|68679|6|Mentioned|p469|Triassic|Triassic|Bowen Basin. Part of the foreland loading during the evolution of the northern New England Orogen.||||||
16052|Rewan Formation|68731|6|Mentioned|p200, p201, p201 Fig 3.110|Middle Triassic|Early Triassic|Galilee Basin. Subdivided in the Bowen Basin and so elevated to Group status (Jensen 1975). Possibly equivalent to the Rewan Group. Written as the Rewan 'Formation' on p201.||||Probably unconformably overlain by the Clematis Formation. Conformably overlain by the Dunda beds.||11-MAY-16
16052|Rewan Formation|69379|5|Briefly described|map legend|Triassic|Triassic|[Not a current name; possibly intended as Arcadia Formation?]||Of Rewan Group|||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16052|Rewan Formation|69594|6|Mentioned|p534|||||||Is overlain unconformably by Eddystone beds.||
16052|Rewan Formation|70821|5|Briefly described|p80|||Basement to Surat Basin.||||Is overlain unconformably by Precipice Sandstone.||14-DEC-16
16052|Rewan Formation|70878|5|Briefly described|p717, p720-721, p725-726|Triassic|Triassic|Bowen Basin. Calibration of palynological ages (D. parvithola Zone). Base of this unit marks the base of the Triassic.||||Unconformably overlies Bandanna Formation.||
16052|Rewan Formation|71265|5|Briefly described|p589-590, p587, p599-600, p602-605|Olenekian|Olenekian|Galilee Basin. Called Rewan Group in the Denison Trough (Bowen Basin). Sedimentary logs of GSQ Muttaburra 1, CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Unconformably overlies Betts Creek Group.||
16052|Rewan Formation|71276|5|Briefly described|p291, p293, p295 Fig.8|Early Triassic|Early Triassic|Galilee Basin.||||Unconformably overlies Bandanna Formation. Is overlain locally by Dunda Beds.||
16052|Rewan Formation|71278|5|Briefly described|p322|Early Triassic|Early Triassic|Bowen Basin. Considered as the reservoir seal in the Fairview Field. 61m thick.|||||Lithic sandstone, mudstone and basal conglomerate.|
16052|Rewan Formation|71701|4|Described|p155, p157-p158, p165-p166, p168-p169|Olenekian|Olenekian|Central Western Area, Galilee Basin; Denison Trough and Northern Area, Bowen Basin. A sample from this unit has a diverse assemblage of palynorphs; palnyology is discussed in some detail. Deposited in a non-marine environment. Intersected in CRD Montani 1, OEC Glue Pot Creek 1, GSQ Tambo 1-1A and GSQ Muttaburra 1.||||Unconformably overlies the Betts Creek Group and Bandanna Formation.||
16052|Rewan Formation|72088|6|Mentioned|p22, p68-p69|Early Triassic|Early Triassic|See Rewan Group.||||||
16052|Rewan Formation|72298|5|Briefly described|p801|||Eromanga (SA,QLD,NSW), Surat Basins. Appears as Rewan Fm./Gp in the SURAT BASIN (QLD,NSW) column on p801.||||Is overlain by Dunda beds or Clematis Sandstone.||
16052|Rewan Formation|73163|6|Mentioned|p468, p472|Triassic|Early Triassic|Galilee Basin. Unclear if Rewan Formation conformably or unconformably overlies the Bandanna Formation, but mudstone bed seen in some places, at boundary.||||Overlies the Bandanna Formation.||
16052|Rewan Formation|73472|6|Mentioned|p115-116|Olenekian|Olenekian|Galilee Basin.||||Overlain by and equivalent to Dunda beds. Equivalent to Rewan Group and Warang Sandstone.||
16054|Rewan Group|13516|5|Briefly described|p145, p159-62, p153,157, 169-70,138,147|Middle Triassic|Late Permian|Of Bowen Basin, Galilee Basin. Age: APP6 - APT 1||||Gradationally overlies Blackwater Group in Denison Trough. Diachronous boundary.||09-MAY-13
16054|Rewan Group|22857|6|Mentioned|p315 Fig. 22.8|||||||||
16054|Rewan Group|22865|6|Mentioned|Fig22.8p315|||||||||
16054|Rewan Group|22973|5|Briefly described|p12|Triassic|Triassic|||||||
16054|Rewan Group|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
16054|Rewan Group|22976|5|Briefly described|p42 Fig.4|Triassic|Triassic|||||||
16054|Rewan Group|22978|6|Mentioned|p148 Fig.1|||||||||
16054|Rewan Group|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
16054|Rewan Group|22984|5|Briefly described|p275|Triassic|Triassic|||||||
16054|Rewan Group|22985|5|Briefly described|p285|Triassic|Triassic|||||||
16054|Rewan Group|22989|5|Briefly described|p310|Triassic|Triassic|||||||
16054|Rewan Group|22995|5|Briefly described|p361|Triassic|Triassic|||||||
16054|Rewan Group|22999|5|Briefly described|p389|Permian|Permian|||||||
16054|Rewan Group|23001|6|Mentioned|p409|||||||||
16054|Rewan Group|23002|5|Briefly described|p417|Triassic|Triassic|||||||
16054|Rewan Group|23005|5|Briefly described|p439|Triassic|Triassic|||||||
16054|Rewan Group|23007|5|Briefly described|p454|Triassic|Triassic|||||||
16054|Rewan Group|23052|5|Briefly described|Map Legend|Triassic|Triassic|||||||
16054|Rewan Group|23060|6|Mentioned|4 fig 2|||Geol province Bowen Basin. Parent Rewan Group||||||
16054|Rewan Group|23161|4|Described|p33 table4 fig11|Triassic|Late Permian|||||||
16054|Rewan Group|23430|5|Briefly described|p514-515|||Bowen Basin Province.||||||
16054|Rewan Group|23444|5|Briefly described|p190|||||||||
16054|Rewan Group|23982|6|Mentioned|p55|||See also Rewan Formation.  Geological Province: Great Artesian Basin.||||||
16054|Rewan Group|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
16054|Rewan Group|24093|5|Briefly described|p177|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16054|Rewan Group|24159|5|Briefly described|p147|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16054|Rewan Group|24241|5|Briefly described|p16|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||
16054|Rewan Group|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
16054|Rewan Group|31079|6|Mentioned|Fig. 6|||||||||
16054|Rewan Group|31401|6|Mentioned|Fig.1|||P30,32||||||
16054|Rewan Group|31690|6|Mentioned|Fig. 2|||||||||
16054|Rewan Group|35433|4|Described|p29|||||||||
16054|Rewan Group|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
16054|Rewan Group|35811|5|Briefly described|Table 5|||||||||
16054|Rewan Group|35901|6|Mentioned|p1|||||||||
16054|Rewan Group|35913|6|Mentioned|p35|||||||||
16054|Rewan Group|35937|6|Mentioned|p619|||||||||
16054|Rewan Group|36104|6|Mentioned|p122|||||||||
16054|Rewan Group|36121|6|Mentioned|p25|||||||||
16054|Rewan Group|36233|6|Mentioned|Table 1|||||||||
16054|Rewan Group|36472|6|Mentioned|Map legend|Triassic|Triassic|||||||
16054|Rewan Group|36739|6|Mentioned|p5|||||||||
16054|Rewan Group|36905|6|Mentioned|p20|||||||||
16054|Rewan Group|36914|6|Mentioned|p87|||||||||
16054|Rewan Group|37274|6|Mentioned|p273|||||||||
16054|Rewan Group|37565|6|Mentioned|p7|||||||||
16054|Rewan Group|37610|6|Mentioned|Fig.3|||||||||
16054|Rewan Group|37612|6|Mentioned|Fig.1|||See also Fig.3.||||||
16054|Rewan Group|37705|6|Mentioned|Fig.1|||||||||
16054|Rewan Group|37724|6|Mentioned|Table 1|||||||||
16054|Rewan Group|37804|6|Mentioned|p63|||||||||
16054|Rewan Group|37996|6|Mentioned|p77|||||||||
16054|Rewan Group|38312|6|Mentioned|p463|||||||||
16054|Rewan Group|38373|6|Mentioned|p614|||||||||
16054|Rewan Group|38374|6|Mentioned|p602|||||||||
16054|Rewan Group|38518|6|Mentioned|Fig.3|||||||||
16054|Rewan Group|38737|6|Mentioned|p156|||||||||
16054|Rewan Group|39212|5|Briefly described|p14|||See also P15||||||
16054|Rewan Group|39252|5|Briefly described|p27|||Perm/Trias boundary||||||
16054|Rewan Group|39269|6|Mentioned|Fig.1|||||||||
16054|Rewan Group|39272|6|Mentioned|p295|||||||||
16054|Rewan Group|39412|6|Mentioned|p1|||See also Fig.11||||||
16054|Rewan Group|39445|5|Briefly described|p115|||||||||
16054|Rewan Group|39491|4|Described|p19|||||||||
16054|Rewan Group|39494|6|Mentioned|Fig.5|||||||||
16054|Rewan Group|39611|6|Mentioned|Fig.3|||||||||
16054|Rewan Group|39815|6|Mentioned|p445|||||||||
16054|Rewan Group|39943|6|Mentioned|Table 5A|||||||||
16054|Rewan Group|40030|6|Mentioned|p135|||See also Fig.5||||||
16054|Rewan Group|40120|4|Described|p425|||||||||
16054|Rewan Group|40245|6|Mentioned|Table 2|||||||||
16054|Rewan Group|40250|6|Mentioned|Table 6|||||||||
16054|Rewan Group|40539|6|Mentioned|Fig.2|||||||||
16054|Rewan Group|40544|6|Mentioned|Fig.6|||||||||
16054|Rewan Group|40574|6|Mentioned|p4|||||||||
16054|Rewan Group|40623|5|Briefly described|p80|||||||||
16054|Rewan Group|40633|6|Mentioned|Fig.1-C|||||||||
16054|Rewan Group|40675|6|Mentioned|p306|||||||||
16054|Rewan Group|41101|6|Mentioned|p294|||||||||
16054|Rewan Group|41102|5|Briefly described|p299|||||||||
16054|Rewan Group|41173|6|Mentioned|p88|||||||||
16054|Rewan Group|41188|6|Mentioned|p231|||||||||
16054|Rewan Group|41191|6|Mentioned|p284|||||||||
16054|Rewan Group|41246|6|Mentioned|Map legend|Triassic||||||||
16054|Rewan Group|41247|6|Mentioned|p127|||||||||
16054|Rewan Group|41481|6|Mentioned|p860|||||||||
16054|Rewan Group|41535|6|Mentioned|Fig.2|||||||||
16054|Rewan Group|41605|6|Mentioned|Fig.2|||||||||
16054|Rewan Group|41893|6|Mentioned|p516|||||||||
16054|Rewan Group|41921|6|Mentioned|Fig.1|||||||||
16054|Rewan Group|42004|6|Mentioned|p150|||||||||
16054|Rewan Group|42008|6|Mentioned|p270|||||||||
16054|Rewan Group|42091|6|Mentioned|Text fig.2 P284|||||||||
16054|Rewan Group|42250|6|Mentioned|Fig.4 P31|||||||||
16054|Rewan Group|42251|6|Mentioned|Fig.2 P38|||||||||
16054|Rewan Group|42257|5|Briefly described|Table 1 P263|||||||||
16054|Rewan Group|42259|6|Mentioned|p18|||||||||
16054|Rewan Group|42437|6|Mentioned|Fig.3 P822|||||||||
16054|Rewan Group|42634|5|Briefly described|Table 2 p10|||||||||05-DEC-22
16054|Rewan Group|42641|5|Briefly described|p109|||||||||
16054|Rewan Group|42701|3|Fully described|p72|||||||||
16054|Rewan Group|42856|5|Briefly described|Fig.2 P632|||||||||
16054|Rewan Group|42865|5|Briefly described|p18|||||||||
16054|Rewan Group|42911|5|Briefly described|p11|||||||||
16054|Rewan Group|42932|5|Briefly described|p69|||||||||
16054|Rewan Group|42999|5|Briefly described|Table 1,p90||Late Permian|||||||
16054|Rewan Group|43000|5|Briefly described|p108|||see also Fig.5,p112||||||
16054|Rewan Group|43002|5|Briefly described|Fig.2,p135|||||||||
16054|Rewan Group|43016|5|Briefly described|p366|||||||||
16054|Rewan Group|43017|5|Briefly described|Fig.3,p375.|||||||||
16054|Rewan Group|43105|5|Briefly described|p13|||||||||
16054|Rewan Group|43185|5|Briefly described|6,10|Triassic|Late Permian|||||||
16054|Rewan Group|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
16054|Rewan Group|43995|14|Not recorded|p40|||||||||
16054|Rewan Group|44245|5|Briefly described|Map Legend||Triassic|||||||
16054|Rewan Group|45095|3|Fully described|p57|||See also p58-60. Used as Rewan Group (Formation) p.8.||||||20-APR-18
16054|Rewan Group|45110|3|Fully described|Table 17|||See also Fig.5 and P24.||||||
16054|Rewan Group|45151|5|Briefly described|Table 10|||See also Table 11. Contains part of former Upper Bowen C.M.||||||
16054|Rewan Group|46937|6|Mentioned|Table 1|||||||||
16054|Rewan Group|46989|5|Briefly described|Table 1|||||||||
16054|Rewan Group|50301|5|Briefly described|Map Legend|Triassic|Triassic|||||||
16054|Rewan Group|60115|5|Briefly described|p21 Fig. 1|Early Triassic|Late Permian|Geological Province: northern Bowen Basin and Comet Ridge.||||||04-FEB-08
16054|Rewan Group|60282|6|Mentioned|p7|Triassic|Triassic|||||||
16054|Rewan Group|60386|6|Mentioned|p296||Early Triassic|Bowen/Sydney Basin. Non-marine.||||||
16054|Rewan Group|60472|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanolithic pebble conglomerate.||||||
16054|Rewan Group|60659|5|Briefly described|p21|Middle Triassic|Late Permian|Sequence of fluviatile sandstone, siltstone and mudstone. Conformably and gradationally overlies the Rangal C.M; conformably overlain by the Clematis Group.  Geological Province: Bowen Basin.||||||07-FEB-11
16054|Rewan Group|61076|5|Briefly described|p188 Fig. 2|Early Triassic|Late Permian|Age: <250Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
16054|Rewan Group|61313|6|Mentioned|p104 Table G1|||||||||
16054|Rewan Group|61377|5|Briefly described|p150|Early Triassic|Early Triassic|Unconformably overlies the Kianga Formation. Geological Province: Surat and Bowen Basins.||||||07-FEB-11
16054|Rewan Group|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Bowen Basin.||||||17-MAR-09
16054|Rewan Group|61782|6|Mentioned|p281, p282|||Geological Province: Taroom Trough. Alluvial and lacustrine sediments.||||||
16054|Rewan Group|62357|5|Briefly described|p524 Fig. 7, p534|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16054|Rewan Group|62921|5|Briefly described|p877-878, p881, p883|Early Triassic|Changhsingian|Jensen (1975) elevated the Rewan Formation in the Bowen Basin to Group status, with two constituent Formations. In the Galilee Basin, the unit remains as the Rewan Formation.|||Includes Arcadia Formation and Sagittarius Sandstone.|Unconformably overlies Blackwater Group. Correlated with Rewan Formation (Galilee Basin).||
16054|Rewan Group|63713|5|Briefly described|p1507 Fig.2, p1512, p1521, p1523, p1528|Early Triassic|Early Triassic|See also p1530 Fig.18, p1533. Galilee and Bowen Basins. Well-log correlation.||||Overlies Betts Creek Beds and Bandana Formation. Is overlain by Clematis Group.||
16054|Rewan Group|63978|5|Briefly described|p7|||Geological province: Bowen Basin. Contact between this Group and the Bandanna Formation represents the traditional lithostratigraphic location of the Permo-Triassic boundary.||||||07-FEB-11
16054|Rewan Group|64099|5|Briefly described|p365, p374 Fig 5|||Includes Sagittarius Sandstone. Geol Prov: Bowen Basin.||||||
16054|Rewan Group|64197|6|Mentioned|p630 Fig.7|Triassic|Permian|||||Underlies the Showgrounds Sandstone; overlies the Blackwater Group.||
16054|Rewan Group|64665|6|Mentioned|p53 Fig.2.|Early Triassic|Early Triassic|Galilee and Bowen Basins.||||Overlies Rangal Coal Measures.||
16054|Rewan Group|64856|3|Fully described|p42, p60-62, p64 Fig.13, p68-73, p78-79|Early Triassic|Late Permian|See also p82, p102. Originally the Rewan Series of Shell (Queensland) Development Pty Ltd (1952), and Isbell (1955). Subsequently Rewan Formation (Hill, 1957); a 515m-thick type section N of Rewan homestead was proposed by Mollan et al. (1969). Upgraded to Group status by Jensen (1975). Bowen and Galilee Basins. Conformably overlies Bandanna Formation and Baralaba Coal Measures. Conformably to disconformably overlain by Clematis Group, Showgrounds Sandstone or Precipice Sandstone. Age from palynoflora (APP6, APT1, APT2). Max thick 1363m. Includes Sagittarius Sandstone and Arcadia Formation. Fine-grained sedimentary rocks.|| ||||29-NOV-17
16054|Rewan Group|64857|4|Described|p124, 126, 134, p113 Fig.3|Early Triassic|Late Permian|Bowen Basin. Contains the Sagittarius Sandstone and Arcadia Formation. Overlies the Bandanna Formation (Denison Trough) and Baralaba Coal Measures (southern Taroom Trough). Age: around the Permian-Triassic boundary, but base is diachronous, younging to east and north.||||||
16054|Rewan Group|64858|6|Mentioned|p180 Fig.2, p181 Tb. 1, p182 Fig.3, p183|Middle Triassic|Early Triassic|Bowen Basin.||||||30-NOV-09
16054|Rewan Group|65112|6|Mentioned|p315, Fig 4 p314|Early Triassic|Late Permian|Supersequence G. Contains sediments 3500 m thick and was deposited over only 2 Ma. Spans the Permian - Triassic boundary.||||Overlies Bandanna Formation of the Denison Trough and Baralaba Coal Measures of the Taroom Trough.||22-MAR-12
16054|Rewan Group|65113|5|Briefly described|p347, Fig 4 p340|Early Triassic|Early Triassic|Underlies the Clematis Group. Includes lithic sandstones. Depositional environment was a meandering river system.||||||18-MAR-13
16054|Rewan Group|65114|5|Briefly described|p385 Fig.3|Early Triassic|Late Permian|||||||
16054|Rewan Group|65115|5|Briefly described|p420, 421, 425, 429, Fig 2 p403|Triassic|Permian|Overlies the Bandanna Formation in the Denison Trough and the Baralaba Coal Measures in the Taroom Trough.  Part of Supersequence G.||||||18-MAR-13
16054|Rewan Group|65116|5|Briefly described|p449, Fig 2 p436|Early Triassic|Late Permian|Overlies the Bandanna Formation of the Denison Trough and the Baralaba CM in the Taroom Trough, Bowen Basin. Equivalent to the Digby Formation, Gunnedah Basin.||||||
16054|Rewan Group|65118|5|Briefly described|p480, 483,491-3, 495-496, Fig 2 p479|Early Triassic|Early Triassic|Overlies the Bandanna Formation in the Denison Trough and the Baralaba Coal Measures in the Taroom Trough, Bowen Basin.||||||
16054|Rewan Group|65119|5|Briefly described|p513, Fig 2, Table 1, Fig 4-12, 14,16,17|Early Triassic|Early Triassic|Bowen Basin. Interbedded sandstone, siltstone, shale, conglomerate. Alluvial deposition up to 570 m thick. Age: 243-248Ma.  Fission Track ages:161-210 Ma. Present in the Cockatoo Creek Well.||||||07-MAR-12
16054|Rewan Group|65388|4|Described|p202-203, p204, p161, p159, 163|Early Triassic|Late Permian|Bowen Basin, Galilee Basin. The Rewan Group (Jensen, 1975) crops out across the entire Bowen Basin and into the Galilee Basin to the west and north. It was formerly named the Rewan Formation (Hill, 1957; Mollan and others, 1969, 1972; Whitaker and others, 1974). No constituent units recognised in the area of this report. Unconformably overlain by Jurassic Precipice Sandstone.||||||09-SEP-14
16054|Rewan Group|65706|4|Described|p12, p16 Tb.1, p18 Tb.1|Early Triassic|Late Permian|Bowen Basin.||||Conformably overlies Blackwater Group; conformably underlies Clematis Group.|Lithic sandstone, pebbly lithic sandstone, siltstone, green to reddish brown mudstone, minor volcanolithic pebble conglomerate (at base).|
16054|Rewan Group|66188|6|Mentioned|441, Fig 3, TB1, Fig 16-17|Middle Triassic|Late Permian|||||||
16054|Rewan Group|66529|6|Mentioned|p12 Fig.5 |||Appears as the ambivalent Rewan Fm/Gp.||||Is overlain by Clematis Sandstone.||
16054|Rewan Group|66615|6|Mentioned|p2 Fig.1, p2-8|||Green (1997). Denison and Southern Taroom Trough, Bowen Basin. Known in company nomenclature as Cabawin Formation.||||||11-JAN-17
16054|Rewan Group|67133|5|Briefly described|p2, p5, p19-21|Triassic|Triassic|Samples of this unit were analysed by XRD and optical microscopy for this study.|||Rewan Formation.|Is overlain by Clematis Group.||
16054|Rewan Group|67402|4|Described|p18 fig WSD2, p21, p30|Induan|Wuchiapingian|Bowen Basin.  Proven hydrocarbon reservoir and potential carbon dioxide storage reservoir. Deposited in a fluvial-lacustrine environment. >100m thick. See also p45, p48, p50 fig BWS4, p53, p55-p57, p60, p62, p65, p72, p80, p85, p85 tbl BWN2, p165 tbl LPB1.||||Unconformably overlain by the Showgrounds Sandstone and the Clematis Group. Overlies the Bandanna Formation and the Rangal Coal Measures.|Lithic sandstone, siltstone and mudstone.|
16054|Rewan Group|67669|5|Briefly described|p11|Early Triassic|Early Triassic|Of Bowen Basin.|||Includes Rewan and Cabawin formations.|Overlain by Mimosa Group. Underlain by Black Water Group.||
16054|Rewan Group|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Unconformably overlies Blackwater Group. Is overlain by Clematis Group.||
16054|Rewan Group|68004|5|Briefly described|p173, p182.|Triassic|Triassic|Low reservoir potential because of extensive silicification and alteration of clays. Acts as a regional seal. Called Rewan Formation on p182.||||||
16054|Rewan Group|68202|6|Mentioned|p176-177|Early Triassic|Early Triassic|Bowen Basin.||||||
16054|Rewan Group|68279|5|Briefly described|p2, p4, p5 Tb.2, p7, p11-12, p16-19|Olenekian|Olenekian|Galilee Basin. Deposited in a fluvio-lacustrine environment. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Is overlain by Clematis Group.|Generally very fine-grained, well to moderately sorted and sub-rounded with medium sphericity. Labile sandstone, siltstone and multi-coloured mudstone.|
16054|Rewan Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin.||||Conformably overlies Blackwater Group. Is overlain conformably by Clematis Group.||
16054|Rewan Group|68576|5|Briefly described|Q_4: p1, p3, p12 Fig.14, p16, p20, p24|Early Triassic|Permian|Bowen Basin. Volcanolithic alluvial sediments sourced from a volcanic arc to the E.|||Sagittarius Sandstone, Arcadia Formation.|Overlies Black Alley Shale and, unconformably, Bandanna Formation. Is overlain unconformably by Clematis Group.|Mainly red-brown, green and khaki mudstones interbedded with green and khaki siltstones and fine- to medium-grained, labile sandstones.|
16054|Rewan Group|68679|5|Briefly described|p312-313, p353, p364, p376,p381,p383-384|Early Triassic|Early Triassic|Throughout the Bowen Basin, northern New England Orogen. Produces gas and minor condensate.||||Overlies Rangal and Baralaba Coal Measures, and Bandanna Formation. Is overlain by the Clematis Group and Showgrounds Sandstone.||
16054|Rewan Group|68731|5|Briefly described|p198, p201 Fig 3.110, p223 Fig 3.126|Middle Triassic|Early Triassic|Bowen Basin. Subdivided in the Bowen Basin and so elevated to Group status (Jensen 1975). Palynological data in the lower part of this Group is Early Triassic.||||Equivalent to the Warang Sandstone.||11-MAY-16
16054|Rewan Group|68901|6|Mentioned|p2 Fig. i|Triassic|Triassic|||||||27-SEP-18
16054|Rewan Group|69379|5|Briefly described|map legend|Triassic|Triassic||||constituent shown as Rewan Formation [possible error?]|||
16054|Rewan Group|69681|6|Mentioned|p82|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
16054|Rewan Group|69760|6|Mentioned|p139|Triassic|Triassic|Bowen Basin. Marks the beginning of the Triassic.||||Overlies the Rangal Coal Measures.||
16054|Rewan Group|69952|6|Mentioned|p85|Triassic|Triassic|||||||
16054|Rewan Group|70673|6|Mentioned|p9|Triassic|Triassic|||||||
16054|Rewan Group|70815|6|Mentioned|p3|||Bowen Basin.||||||
16054|Rewan Group|70878|5|Briefly described|p705|||Bowen Basin. A CA-IDTIMS age of 252.2 +/- 0.4 Ma for this unit by Mundil et al. (2006) is discussed with reference to an earlier SHRIMP age determination of 250.1 +/- 2.8 Ma by Roberts et al. (1996) for the stratigraphically lower [sic] Black Alley Shale, allowing that unit a late Permian or Early Triassic age.||||||
16054|Rewan Group|71265|5|Briefly described|p589-590|Olenekian|Induan|Denison Trough, Bowen Basin. Called Rewan Formation in the Galilee Basin.||||Unconformably overlies Bandanna Formation.||
16054|Rewan Group|71710|5|Briefly described|p370, 380, 381, 382, 383, 385, 386, 387|Late Permian|Late Permian|Bowen Basin? Geological province: Galilee Basin. Depositional environment, well log character and sequence stratigraphy described. Provenance is from recycled western orogen source and volcaniclastic input.||Part sequence 6, sequence 7.||Unconformably overlain by Clematis Group (discontinuous relationship in seismic). Underlain by Betts Creek beds.||
16054|Rewan Group|72088|4|Described|p8, p15, p21-p22, p91|Anisian|Induan|Southern and Eastern Galilee Basin and Bowen Basin. Sediments in the southeast of the basin are generally fine-grained with medium-grained layers and are well- to moderately-sorted.||||Unconformably overlies the Bandanna Formation. Conformably overlain by the Dunda beds. Unconformably overlain by the Clematis Group.|Quartzose sandstone, siltstone and mudstone.|
16054|Rewan Group|72297|5|Briefly described|p694 Fig.10.8, p744-745|||Bowen Basin. Hydrocarbon reservoir quality is generally poor, but improves southwards where sandstones are more quartzose.||||Overlies Rangal Coal Measures.||
16054|Rewan Group|73036|5|Briefly described|Map legend|Middle Triassic|Early Triassic||||||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16054|Rewan Group|73037|5|Briefly described|Map legend|Middle Triassic|Early Triassic||||||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16054|Rewan Group|73038|5|Briefly described|Map legend|Middle Triassic|Early Triassic||||||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16054|Rewan Group|73040|5|Briefly described|Map legend|Middle Triassic|Early Triassic||||||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16054|Rewan Group|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 49, 88, 98...|||Bowen Basin. Tight aquitard. More locations: p. 115, 117, 119, 146, 151-153, 169-172, 177, 179, 191.||||Underlain by Bandanna Formation. Overlain by Clematis Sandstone and unconformably by Precipice Sandstone.||
16054|Rewan Group|73246|6|Mentioned|p190-191|Lower Triassic|Lower Triassic|Bowen Basin.||||Underlain by Rangal Coal Measures (Blackwater Group). Overlain by Clematis Group.||
16054|Rewan Group|73304|6|Mentioned|p61, p71-72, p76-78|Induan|Changhsingian|Bowen Basin. End-Permian mass extinction is recognised close to the base of this unit. Lower portion correlates to the GSSP-defined P-T boundary. [Basal?] boundary marks a major extinction of peat-producing plants.|||Sagittarius Sandstone|||
16054|Rewan Group|73472|5|Briefly described|p115, p120, p129, p131, App.1|Olenekian|Induan|Bowen Basin. Not represented in the northeastern Galilee Basin. Previously thought to occur within Porcupine Gorge; however, these strata are younger and were formalized as the Porcupine Gorge Formation.||||Underlain by Bandana Formation. Overlain by Clematis Group. Equivalent to Rewan Formation.||
16054|Rewan Group|73570|5|Briefly described|p914, p916, p919 Fig.6|Early Triassic|Early Triassic|Bowen Basin. See also Rewang Group p915 Fig.4.|||||Alluvial plain. Includes fluviatile, quartz-rich sandstones.|
16054|Rewan Group|73625|6|Mentioned|p2-3, p5 Fig.3, p14, 22, p26|Early Triassic|Early Triassic|See also p23 Fig.14F. Bowen Basin. Graphic sedimentary logs. Deposition in a lowland alluvial plain. Work by several cited authors indicates the Permian/Triassic boundary occurs within [sic] the lower beds of this Group.|||Arcadia Formation.|Overlies 'Marker Mudstone'/Bandanna Formation.||
16070|Rhyolite Range beds|22601|4|Described|415|Permian|Permian|Within Silverwood Block. Thickness >1200 m. Overlain by Marburg Sandstone; underlain by Rosenthal Creek Formation.||||||12-DEC-07
16070|Rhyolite Range beds|39252|6|Mentioned|p22|||||||||
16070|Rhyolite Range beds|42994|6|Mentioned|p43|||||||||
16070|Rhyolite Range beds|43008|5|Briefly described|map legend|||||||||
16070|Rhyolite Range beds|43017|6|Mentioned|p377|||||||||
16070|Rhyolite Range beds|61392|5|Briefly described|p164 Fig. 1|Late Permian|Late Permian|Of the Wildash Group.||||||07-FEB-11
16070|Rhyolite Range beds|63731|5|Briefly described|Map legend|Permian|Permian|Arenite+siltstone; some conglomerate. Locally spherulitic rhyolite sills and flows, agglomerate, crystal tuff, quartz-feldspar porphyry + minor dacitic to andesitic lava. Siliceous pebbly orthoconglom. Fossiliferous/bioturbated litharenite and siltstone.||||||
16070|Rhyolite Range beds|63748|4|Described|p7 Fig. 3, p20|Late Permian|Middle Permian|Of Olgers et al (1974) - redefined by Dennis (1974a). Unconformable on Silverwood Group rocks; unconformable below Marburg Subgroup. Max. thickness:1300m. Mainly felsic volcanics. Detailed lithology provided. Geological province: Wandsworth Province.||||||07-FEB-11
16070|Rhyolite Range beds|68679|5|Briefly described|p446, p453|Permian|Permian|Mapped by Olgers et al. (1974) but redefined by Dennis (1974); the extent of the unit was modified by Van Noord (1999). Silver Spur Subprovince, Woolomin Province. Forms a narrow elongate belt 10km S of Warwick. >1300m thick. Contains a middle Permian marine fauna.||Wildash Group.||Unconformably overlies or is faulted against the Silverwood Group. Is overlain unconformably by the Marburg Subgroup. May correlate with Fitz Creek beds.|Mainly felsic volcanics, including spherulitic rhyolite sills (and flows?), breccia, crystal tuff, quartz-feldspar porphyry, and minor dacitic to andesitic lava; ~120-300m of locally pebbly lithic sandstone and siltstone at the base.|
16070|Rhyolite Range beds|71628|6|Mentioned|p16:4|||||||Is intruded by Cullendore Syenogranite.||
16093|Ridgelands Granodiorite|23799|5|Briefly described|p117|||Of Murray et al (2000, in prep.).  Of the Monal Suite.  Geological Province: Yarrol Province.||||||
16093|Ridgelands Granodiorite|24615|5|Briefly described|CD|Early Triassic|Late Permian|[PRgri].  Grey medium-grained biotite-hornblende to hornblende-biotite granodiorite, grey to cream medium-grained biotite-hornblende tonalite to quartz diorite, locally xenolith-bearing.||||||
16093|Ridgelands Granodiorite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
16093|Ridgelands Granodiorite|31657|6|Mentioned|p95|||||||||
16093|Ridgelands Granodiorite|31658|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16093|Ridgelands Granodiorite|31659|4|Described|p89|Permian|Permian|Even grained, white rock speckled with black mafic minerals. More lithological details included.||||||09-JUN-09
16093|Ridgelands Granodiorite|32358|4|Described|Table 4|||P17||||||
16093|Ridgelands Granodiorite|32944|6|Mentioned|p703|||260m.y. Footnote.||||||
16093|Ridgelands Granodiorite|34574|6|Mentioned|p115|||||||||
16093|Ridgelands Granodiorite|36045|6|Mentioned|p333|||See also Fig.4.||||||
16093|Ridgelands Granodiorite|36576|6|Mentioned|p613|||||||||
16093|Ridgelands Granodiorite|38081|5|Briefly described|Table 2|||||||||
16093|Ridgelands Granodiorite|38406|6|Mentioned|p13|||||||||
16093|Ridgelands Granodiorite|39252|5|Briefly described|p22|||||||||
16093|Ridgelands Granodiorite|39445|5|Briefly described|p106|||Mid Permian. See also Table 12||||||
16093|Ridgelands Granodiorite|40787|6|Mentioned|p371|||||||||
16093|Ridgelands Granodiorite|41246|6|Mentioned|Map legend|Permian||||||||
16093|Ridgelands Granodiorite|41922|4|Described|Table 2, P13|||||||||
16093|Ridgelands Granodiorite|50209|5|Briefly described|Map Legend|Triassic|Permian|||||||
16093|Ridgelands Granodiorite|60557|5|Briefly described|p19 Fig. 5b, p27|Late Triassic|Late Permian|Geochemically part of the Clarence River Supersuite.  Hornblende-bearing I-type granitoid dominated by granodiorite, tonalite and quartz diorite.  Intruded the Craigilee beds.||||||09-JUN-05
16093|Ridgelands Granodiorite|68008|2|Defined|p11-12, p17, p254, p261, p307, p330,p334|Early Triassic|Permian|See also p337-340, p390-393, p484, p530, p565. Kirkegaard et al. (1970). Previously included the Wattlebank Granodiorite. Named after Ridgelands Creek. Crops out as a 115 km2 boomerang-shaped body, centred 20km NW of Rockhampton, and a smaller (c.10 km2) mass around Sugarloaf Mountain. The type area appears to be outcrops between Station Creek and Two Mile Creek (GR040 288 on the Ridgelands sheet). Undulating to hilly topography. Geophysics described in some detail. Geochemistry described: very similar to Wattlebank Granodiorite. Intrudes serpentinite on the south bank of the Fitzroy River near Eden Bann homestead. Previous ages of 269 Ma, 264 Ma (K-Ar hornblende; Webb, 1969) are from outcrops now included in Wattlebank Granodiorite. Post-tectonic. Probable source of gold mineralisation at Morinish, Ridgelands and Rosewood. Rb-Sr data tabulated.|251 +/- 2 Ma (biotite-whole rock).|||Intrudes Craigilee beds; Mount Alma, Neerkol Formations; Youlambie Conglomerate, and Rockhampton Group. Is overlain nonconformably by Dalma Basalt and Mount Salmon Volcanics.|Dominantly equigranular granodiorite and tonalite, locally intruded by biotite-bearing microgranite, diorite and gabbro. Local intrusion and dykes of biotite microgranite; 3 local gabbro-diorite bodies. The smaller outcrop is more mafic.|
16093|Ridgelands Granodiorite|68679|5|Briefly described|p314, p410, p424, p426-427|||Yarrol Province. A boomerang-shaped, ~115 km2 multiphase batholith between Ridgelands and Mount Salmon with a smaller body near Sugarloaf Mountain. Separates two small exposures of the Morinish Belt in the Craigilee Subprovince. Hosts gold mineralisation. Geochemistry briefly described.|251 +/- 2 Ma (U-Pb zircon: Fanning, 2012).||||Biotite-hornblende to hornblende-biotite granodiorite, biotite-hornblende tonalite to quartz diorite. Intruded by small diorite-gabbro and microgranite/microsyenite bodies.|
16093|Ridgelands Granodiorite|69952|6|Mentioned|p75|Early Triassic|Permian|||||||
16095|Rifle Creek beds|38350|6|Mentioned|p9|||||||||
16095|Rifle Creek beds|39445|6|Mentioned|p39|||||||||
16095|Rifle Creek beds|45161|6|Mentioned|p22|||||||||
16095|Rifle Creek beds|46859|6|Mentioned|p313|||Informal name.||||||
16095|Rifle Creek beds|46962|6|Mentioned|p248|||||||||
16095|Rifle Creek beds|46996|6|Mentioned|p273|||||||||
16116|Risdon Stud Formation|31999|6|Mentioned|Table 1|||||||||
16116|Risdon Stud Formation|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian?  to Lower Devonian. Of Silverwood Group.||||||25-OCT-05
16116|Risdon Stud Formation|32672|6|Mentioned|p673|||||||||
16116|Risdon Stud Formation|33146|5|Briefly described|p2|||See also p3. ?Sil.-L.Dev.||||||07-SEP-18
16116|Risdon Stud Formation|33703|6|Mentioned|p207|||||||||
16116|Risdon Stud Formation|35311|6|Mentioned|p207|||||||||
16116|Risdon Stud Formation|35652|4|Described|p6|||||||||
16116|Risdon Stud Formation|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
16116|Risdon Stud Formation|39071|6|Mentioned|p345|||||||||
16116|Risdon Stud Formation|39445|5|Briefly described|Table 5,p77|||||||||25-OCT-05
16116|Risdon Stud Formation|42031|5|Briefly described|Fig.3 P759|||||||||
16116|Risdon Stud Formation|48940|3|Fully described|p24|||||||||
16116|Risdon Stud Formation|61392|4|Described|p163-165, p166|Pridoli|Middle Cambrian|Of the Silverwood Group (Keinjan Terrane). Represents a normal clastic or mixed mud and mud/sand-rich slope apron. Age: 512-414Ma. Max. thickness: ~2500m.||||||07-FEB-11
16116|Risdon Stud Formation|63731|5|Briefly described|Map legend|Devonian|Silurian|Of the Silverwood Group. Silicified, fine-gr., cherty, andesitic crystal-lithic tuff, interbedded with subordinate thin to medium bedded, fine-gr. silicified arenite and mudstone (turbidites).||||||12-DEC-07
16116|Risdon Stud Formation|63748|4|Described|p6, p7 Fig. 3|Middle Silurian|Early Cambrian|Of Silverwood Group. Conformable below Connolly Volcanics. Max.thickness: ~2500m. Geol.Prov:Silverwood Prov.Silicified, fine-gr.cherty pyroclastic andesitic crystal-lithic tuffs, interbedded + subordinate thin-medium bedded, fine-gr.silicified turbidites.||||||07-FEB-11
16116|Risdon Stud Formation|68679|5|Briefly described|p445-447|Silurian|Silurian|Olgers et al. (1974). Silverwood Province. ~2500m thick. Age discussed.||Basal Silverwood Group.||Is overlain by Connolly Volcanics.|Cherty andesitic crystal-lithic tuff, and subordinate thin- to medium-bedded turbidites.|
16116|Risdon Stud Formation|71628|5|Briefly described|p19: 59, 67|||||Silverwood Group.||Is intruded by Herries Monzogranite.|Silicified, fine-grained, cherty, andesitic crystal-lithic tuff, interbedded with subordinate thin- to medium-bedded, fine-grained, silicified arenite and mudstone (turbidites).|
16135|Riversdale Formation|30242|6|Mentioned|Fig.2|||||||||
16135|Riversdale Formation|30479|6|Mentioned|Fig.6|||||||||
16135|Riversdale Formation|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
16135|Riversdale Formation|33111|6|Mentioned|p38|||||||||
16135|Riversdale Formation|33900|6|Mentioned|p19|||||||||
16135|Riversdale Formation|35054|6|Mentioned|p246|||||||||
16135|Riversdale Formation|35074|6|Mentioned|Fig.2|||||||||
16135|Riversdale Formation|37572|6|Mentioned|p157|||See also Fig.8||||||
16135|Riversdale Formation|37816|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
16135|Riversdale Formation|38350|6|Mentioned|p22|||||||||
16135|Riversdale Formation|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
16135|Riversdale Formation|38446|6|Mentioned|p144|||||||||
16135|Riversdale Formation|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16135|Riversdale Formation|39445|5|Briefly described|Table 4|||See also p61 and p62.||||||28-NOV-06
16135|Riversdale Formation|39690|6|Mentioned|Table 1|||||||||
16135|Riversdale Formation|40038|6|Mentioned|Fig.1|||||||||
16135|Riversdale Formation|40856|6|Mentioned|Fig.23.6|||||||||
16135|Riversdale Formation|44211|14|Not recorded|p96,102|||Rests on basement and forms residuals below Thorntonia Limestone.||||||
16135|Riversdale Formation|44271|14|Not recorded|p21-62|||Not listed on white card.||||||
16135|Riversdale Formation|44273|14|Not recorded|Map Legend||Neoproterozoic|||||||
16135|Riversdale Formation|44275|14|Not recorded|Map Legend|||||||||
16135|Riversdale Formation|44309|2|Defined|Tb.1,opp.p7,7-9,map|||No fossils. Overlies Precambrian unconformably.||||||
16135|Riversdale Formation|44326|14|Not recorded|Map Legend||Early Cambrian|||||||
16135|Riversdale Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Cambrian|||||||
16135|Riversdale Formation|44989|4|Described|p.125|||Tb.II. (F54-5).||||||
16135|Riversdale Formation|45012|14|Not recorded|p26,27||Early Cambrian|||||||
16135|Riversdale Formation|45052|5|Briefly described|p74|||L.Camb.||||||
16135|Riversdale Formation|45079|5|Briefly described|p10|||Precambrian age. See also p16,p28,p29. Term to be discontinued.||||||28-NOV-06
16135|Riversdale Formation|45166|5|Briefly described|Table 15|||||||||
16135|Riversdale Formation|45287|14|Not recorded|p.223||Cambrian|||||||
16135|Riversdale Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
16135|Riversdale Formation|46955|6|Mentioned|p159|||||||||
16135|Riversdale Formation|47058|6|Mentioned|Fig.8 P129|||||||||
16135|Riversdale Formation|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, sandy dolomite, siltstone, mudstone, conglomerate.||||||
16135|Riversdale Formation|64068|4|Described|p54, 58, 225|Early Cambrian|Early Cambrian|To 30 m thick. Forms mesa cappings and low scarps. Correlations depend on boundary relations.||Of Shadow Group.||Is overlain by Thorntonia Limestone either unconformably or conformably and gradationally.|Conglomerate, red sandstone and red quartzic dolostone.|05-APR-12
16135|Riversdale Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cambrian|Neoproterozoic|Georgina Basin||Shadow Group|||Conglomerate, arenite, arkose, shale, mudstone, dolomite|
16135|Riversdale Formation|69443|5|Briefly described|p28:7, 14, 16|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||Is overlain by Thorntonia Limestone unconformably or gradationally[?].||12-JUL-16
16135|Riversdale Formation|69591|5|Briefly described|p90, p97, p98 Fig.2.91|Cambrian|Neoproterozoic|Oban Sub-basin, Georgina Basin. Crops out only in the Ardmore outlier as erosional residuals up to 30m thick.||Shadow Group.||Is overlain conformably by Thorntonia Limestone. Notional correlative of Mount Birnie beds.|Red sandstone, with several conglomerate bands in the lower part and red sandy dolomite above. Unfossiliferous.|
16145|Riverstone Sandstone Member|13516|5|Briefly described|p145 fig 3, p146 fig 4, p150|Early Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP3101. Coastal lagoon.||Cattle Creek Formation||||
16145|Riverstone Sandstone Member|24077|5|Briefly described|p412 Fig. 8|Early Permian|Early Permian|Of Cattle Creek Formation.  Geological Province: Bowen Basin.||||||
16145|Riverstone Sandstone Member|29721|6|Mentioned|Table 65|||||||||
16145|Riverstone Sandstone Member|30826|6|Mentioned|Fig.1|||||||||
16145|Riverstone Sandstone Member|31120|4|Described|p150|||||||||
16145|Riverstone Sandstone Member|32139|6|Mentioned|p582|||See Table||||||
16145|Riverstone Sandstone Member|32577|5|Briefly described|p23|||See also P24. L.Perm.||||||
16145|Riverstone Sandstone Member|32840|6|Mentioned|Fig.2|||See also P29 - Stratigraphy & biostratigraphy||||||
16145|Riverstone Sandstone Member|35148|6|Mentioned|p411|||||||||
16145|Riverstone Sandstone Member|35457|6|Mentioned|Fig.4|||l||||||
16145|Riverstone Sandstone Member|36243|6|Mentioned|Table 3A|||||||||
16145|Riverstone Sandstone Member|36739|6|Mentioned|p19|||||||||
16145|Riverstone Sandstone Member|37705|6|Mentioned|Fig.2|||||||||
16145|Riverstone Sandstone Member|37726|3|Fully described|p142|||||||||
16145|Riverstone Sandstone Member|39219|6|Mentioned|p46|||Microflora||||||
16145|Riverstone Sandstone Member|39262|6|Mentioned|p130|||See also P134||||||
16145|Riverstone Sandstone Member|39263|6|Mentioned|p146|||||||||
16145|Riverstone Sandstone Member|39273|6|Mentioned|p305|||||||||
16145|Riverstone Sandstone Member|39943|6|Mentioned|Table 5A|||||||||
16145|Riverstone Sandstone Member|40093|6|Mentioned|p38|||||||||
16145|Riverstone Sandstone Member|41605|6|Mentioned|Fig.2|||||||||
16145|Riverstone Sandstone Member|42578|6|Mentioned|Table 1 P124-125|||Actually spelt Riverstone Ss Mb.||||||
16145|Riverstone Sandstone Member|43050|5|Briefly described|p16|||||||||
16145|Riverstone Sandstone Member|44172|4|Described|Tb.1,p1331,1336||Artinskian|Springsure area.||||||
16145|Riverstone Sandstone Member|44173|2|Defined|p109-113,115||Artinskian|Formerly Stanleigh Formation and mudstone. Conformably overlain by Staircase Sandstone Member. Member of Cattle Creek Formation.||||||
16145|Riverstone Sandstone Member|45071|6|Mentioned|p40|||Refers Power (1966)||||||
16145|Riverstone Sandstone Member|46849|6|Mentioned|Fig. 7|||||||||
16145|Riverstone Sandstone Member|48900|6|Mentioned|Table 3|||||||||
16145|Riverstone Sandstone Member|68576|5|Briefly described|Q_4: p19|Permian|Permian|Denison Trough.||Cattle Creek Formation.||||
16164|Roaring Siltstone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, fine sandstone, chert. Underlies: Devoncourt Limestone, O'Hara Shale. Overlies: Thorntonia Limestone.||||||27-AUG-04
16164|Roaring Siltstone|22954|6|Mentioned|Fig3p9|Boomerangian|Undillan|||||||
16164|Roaring Siltstone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
16164|Roaring Siltstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|31396|6|Mentioned|Fig.3|||||||||
16164|Roaring Siltstone|32952|6|Mentioned|p1188|||See also p1189. M.-U. Camb.||||||28-NOV-06
16164|Roaring Siltstone|33111|4|Described|p41|||Mention p6.||||||28-NOV-06
16164|Roaring Siltstone|33113|6|Mentioned|Fig.1|||Middle Camb.||||||
16164|Roaring Siltstone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
16164|Roaring Siltstone|34903|6|Mentioned|p582|||||||||
16164|Roaring Siltstone|35054|6|Mentioned|Table 23|||||||||
16164|Roaring Siltstone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|35139|4|Described|Table.2|||||||||
16164|Roaring Siltstone|35553|6|Mentioned|p153|||||||||
16164|Roaring Siltstone|35939|6|Mentioned|p633|||||||||
16164|Roaring Siltstone|36234|6|Mentioned|p168|||||||||
16164|Roaring Siltstone|37275|6|Mentioned|p290|||||||||
16164|Roaring Siltstone|37413|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|37572|4|Described|p159|||See also Fig.8||||||
16164|Roaring Siltstone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|38350|6|Mentioned|p22|||||||||
16164|Roaring Siltstone|38444|6|Mentioned|p139|||||||||
16164|Roaring Siltstone|38446|6|Mentioned|Table 23|||||||||
16164|Roaring Siltstone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16164|Roaring Siltstone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|Overlain by O'Hara Shale.||||||25-AUG-04
16164|Roaring Siltstone|39445|5|Briefly described|Table 4|||See also p62.||||||28-NOV-06
16164|Roaring Siltstone|39690|6|Mentioned|Table 1|||See also Fig.2||||||
16164|Roaring Siltstone|40852|6|Mentioned|Fig.3.7|||||||||
16164|Roaring Siltstone|40856|5|Briefly described|p313|||||||||
16164|Roaring Siltstone|41306|6|Mentioned|p4|||||||||
16164|Roaring Siltstone|41388|6|Mentioned|Fig.2|||||||||
16164|Roaring Siltstone|42139|6|Mentioned|Fig.18 P90|||||||||
16164|Roaring Siltstone|44205|2|Defined|p9-13,26-7,31-7,40-7||Middle Cambrian|p51-9,74-87,135,164,180-85. Overlies Mount Birnie Beds. Overlain by Devoncourt Limestone.||||||
16164|Roaring Siltstone|44211|14|Not recorded|p96,104,107|||||||||
16164|Roaring Siltstone|44275|14|Not recorded|Map Legend|||||||||
16164|Roaring Siltstone|44276|2|Defined|p21,Tb.2,map|||||||||
16164|Roaring Siltstone|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
16164|Roaring Siltstone|44278|14|Not recorded|Tb.1|||||||||
16164|Roaring Siltstone|44757|6|Mentioned|p155|||Probable stratigraphic equivalent of Beetle Creek Formation.||||||
16164|Roaring Siltstone|44882|14|Not recorded|p201||Cambrian|In French.||||||28-NOV-06
16164|Roaring Siltstone|45052|2|Defined|p101|Middle Cambrian|Middle Cambrian|||||||
16164|Roaring Siltstone|45079|5|Briefly described|p30|||Cambrian age||||||
16164|Roaring Siltstone|45166|5|Briefly described|Table 15|||||||||
16164|Roaring Siltstone|47058|6|Mentioned|Fig.4 P124|||||||||
16164|Roaring Siltstone|48633|14|Not recorded|p99|||Ref. to Opik 1961.||||||
16164|Roaring Siltstone|50100|5|Briefly described|p22|Early Ordovician|Early Cambrian|Finely laminated siltstone, siliceous shale and fine-grained sandstone.  Disconformably overlies Thorntonia Limestone; overlain conformably by (and passes laterally into) Devoncourt Limestone.||||||
16164|Roaring Siltstone|60122|6|Mentioned|p57 Appendix|||Geological Province: Burke River Structural Belt. Correlated with parts of the Arthur Creek Formation.||||||
16164|Roaring Siltstone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Siltstone, sandstone; minor chert, shale.||||||
16164|Roaring Siltstone|63450|5|Briefly described|p78 Fig. 5|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
16164|Roaring Siltstone|64068|3|Fully described|p64, 62, 63|Middle Cambrian|Middle Cambrian|Contains trilobites, brachiopods, molluscs, sponges and archaeocopides. Correlations: Age Creek Formation, V Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Currant Bush Limestone, Devoncourt Limestone in part, Blazan Shale, Quita Formation, Camooweal Dolostone, upper Arthur Creek Formation.||Of Narpa Group.||Conformably overlies Inca Formation. Disconformable over Beetle Creek Formation or Thorntonia Limestone. Interdigitates with and is overlain by Devoncourt Limestone.|Siliceous shale, siltstone, sandstone; local basal conglomerate.|04-APR-12
16164|Roaring Siltstone|64443|6|Mentioned|p41|||Undilla Sub-basin. Correlative of Ranken Limestone, Camooweal Dolostone.||||||
16164|Roaring Siltstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin.||Narpa Group.||Unconformably overlies Inca Formation. Is overlain by Devencourt Limestone.|Siltstone, sandstone; minor chert, silicified shale.|
16164|Roaring Siltstone|67870|6|Mentioned|p43|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin.||||||
16164|Roaring Siltstone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Siltstone and sandstone; minor chert and silicified shale|
16164|Roaring Siltstone|69443|5|Briefly described|p28:16, 24-25|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Ranken Limestone and Camooweal Dolostone.||12-JUL-16
16164|Roaring Siltstone|69573|6|Mentioned|p659, 661, 666, 668|||Georgina Basin. Deeper water, mid-outer shelf and slope settings.||||Grades laterally and vertically into Devoncourt Limestone.||
16164|Roaring Siltstone|69591|5|Briefly described|p87, p92, p96-97, p98 Fig.2.91|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. Up to 70m thick. Lithologically identical to Inca Formation; considered to be its northern younging extension. They are distinguished by fossil fauna (named).||||Unconformably overlies Thorntonia Limestone. Is overlain conformably by, and passes laterally into, Devoncourt Limestone.|Thin-bedded, silty, siliceous shale with minor thin chert and fine sandstone and some bituminous calcilutites.|
16164|Roaring Siltstone|72321|6|Mentioned|Fig 2|Guzhangian|Drumian|Burke River Structural Belt, Georgina Basin. Australian stages:  Undillan to Boomerangian.||of Narpa Group.||||
16164|Roaring Siltstone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
16164|Roaring Siltstone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Underlies and is equivalent to Devoncourt Limestone. Unconformably overlies Thorntonia Limestone.|Siltstone and sand stone; minor chert and silicified shale.|
16164|Roaring Siltstone|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Overlies Thorntonia Limestone and underlies Devoncourt Limestone.|Siltstone and sandstone; minor chert and silicified shale.|
16164|Roaring Siltstone|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Lateral equivalent of Inca Formation, underlies Selwyn Range Limestone, Devoncourt Limestone|Siltstone.|
16185|Robin Hood Granodiorite|9541|5|Briefly described|Map legend|Devonian|Silurian|Pink to grey hornblende-biotite granodiorite with quartz phenocrysts.||||||
16185|Robin Hood Granodiorite|22669|6|Mentioned|P249|||||||||
16185|Robin Hood Granodiorite|23220|5|Briefly described|Fig.1,2 p13|Early Devonian|Late Silurian|Contains large roof pendant of Daniel Creek Formation and Digger Creek Granite. of Georgetown Inlier.||||||
16185|Robin Hood Granodiorite|23291|4|Described|p89 Fig. 3.8|Early Devonian|Early Devonian|Parent: White Springs Supersuite. Age: >407Ma. Geological Province: Georgetown Region.||||||28-MAY-15
16185|Robin Hood Granodiorite|23513|5|Briefly described|Map legend|Devonian|Silurian|Palaeozoic Intrusive No. 31. I-Type.||||||
16185|Robin Hood Granodiorite|23619|5|Briefly described|p7|Devonian|Silurian|||||||
16185|Robin Hood Granodiorite|29613|6|Mentioned|p103|||See also Fig.1||||||
16185|Robin Hood Granodiorite|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
16185|Robin Hood Granodiorite|33907|6|Mentioned|p5|||||||||
16185|Robin Hood Granodiorite|33909|1|Redefined|p230|Devonian|Silurian|Silurian or Devonian||||||
16185|Robin Hood Granodiorite|35920|6|Mentioned|p21|||Defined by Withnall & others 1976.||||||
16185|Robin Hood Granodiorite|35921|6|Mentioned|p34|||||||||
16185|Robin Hood Granodiorite|36153|6|Mentioned|Table 2|||||||||
16185|Robin Hood Granodiorite|37570|4|Described|p120|||See also Fig.3||||||
16185|Robin Hood Granodiorite|37571|5|Briefly described|p137|||||||||
16185|Robin Hood Granodiorite|37576|5|Briefly described|p8|||||||||
16185|Robin Hood Granodiorite|37614|4|Described|p237|||||||||
16185|Robin Hood Granodiorite|38752|6|Mentioned|p43|||||||||
16185|Robin Hood Granodiorite|39147|6|Mentioned|p234|||||||||
16185|Robin Hood Granodiorite|39445|5|Briefly described|Table 12|||Part renamed Mt Hogan Granite. See also P72||||||
16185|Robin Hood Granodiorite|39687|6|Mentioned|p3|||||||||
16185|Robin Hood Granodiorite|39917|6|Mentioned|Map legend|Late Silurian|Late Silurian|Late Silurian-Early Devonian||||||
16185|Robin Hood Granodiorite|39981|6|Mentioned|p105|||||||||
16185|Robin Hood Granodiorite|41272|5|Briefly described|M 1of1 B06|||||||||
16185|Robin Hood Granodiorite|41680|6|Mentioned|p104|||||||||
16185|Robin Hood Granodiorite|43259|4|Described|Appendix 1,p17.|Early Devonian|Late Silurian|||||||
16185|Robin Hood Granodiorite|43664|6|Mentioned|p94|||||||||
16185|Robin Hood Granodiorite|45113|6|Mentioned|p33|||||||||
16185|Robin Hood Granodiorite|50199|5|Briefly described|Map Legend|Late Silurian|Late Silurian|||||||
16185|Robin Hood Granodiorite|50211|5|Briefly described|Map Legend|Late Silurian|Late Silurian|Pink to grey hornblende-biotite granodiorite with quartz phenocrysts.||||||
16185|Robin Hood Granodiorite|68353|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Robin Hood Batholith, Pama Province.|||||Pink to grey hornblende-biotite granodiorite with quartz phenocrysts.|
16185|Robin Hood Granodiorite|68357|5|Briefly described|Map legend.|Late Silurian|Late Silurian|Pama Province.|||||Pink to grey hornblende-biotite granodiorite with quartz phenocrysts.|
16185|Robin Hood Granodiorite|69592|5|Briefly described|p282, p285|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
16185|Robin Hood Granodiorite|72297|5|Briefly described|p710|Silurian|Silurian|Agate Creek. Asssociated with epithermal gold deposits in reactivated faults.||||||
16185|Robin Hood Granodiorite|72983|6|Mentioned|p70, p74|Frasnian|Gorstian|Rb-Sr age of ~426 Ma from Black (1973). K-Ar age of ~380 Ma from Richards et al. (1966).|~426 Ma and ~380 Ma|||Cut by an unnamed rhyolite sill from Sherwood gold deposit.||
16185|Robin Hood Granodiorite|73387|6|Mentioned|p9, p20|Late Devonian|Silurian|Intruded by rhyolite dykes at the historic Homeward Bound gold mine. Biotite K-Ar age of c. 380 Ma from Richards et al. (1966) and biotite Rb-Sr age of c. 426 Ma from Black (1973).|c. 380 Ma K-Ar, c. 426 Ma Rb-Sr|||||
16201|Rockfields Member|22800|5|Briefly described|Fig.14 p592|Frasnian|Frasnian|of Bundock Creek Group||||||
16201|Rockfields Member|23032|5|Briefly described|p30|||||||||
16201|Rockfields Member|23424|5|Briefly described|Table 8.1 p336.||Late Devonian|Age: Frasnian?; marine fossils. Very similar to Vanneck Formation in Burdekin Basin. Of Bulgeri Formation/Bundock Creek Group, Bundock Basin.||||||
16201|Rockfields Member|24613|5|Briefly described|p133|||Part of a unit of the Bundock Creek Group. Contains numerous tuffs.||||||21-JUN-13
16201|Rockfields Member|41260|3|Fully described|p81|||Reserved as Rockfields Formation.||||||25-MAR-08
16201|Rockfields Member|41679|6|Mentioned|Fig.2|||||||||
16201|Rockfields Member|41719|6|Mentioned|Fig.2|||||||||
16201|Rockfields Member|41739|2|Defined|p301|Famennian|Frasnian|||||||
16201|Rockfields Member|41740|6|Mentioned|p222|||||||||
16201|Rockfields Member|42054|6|Mentioned|p273|||||||||
16201|Rockfields Member|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
16201|Rockfields Member|42709|6|Mentioned|map legend|||||||||
16201|Rockfields Member|42933|4|Described|p129|||Of Bulgeri Formation.||||||27-MAY-09
16201|Rockfields Member|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bulgeri Formation.||||||
16201|Rockfields Member|67788|6|Mentioned|p22|Late Devonian|Late Devonian|Mentioned in a list of units containing braided and low-sinuosity river deposits.||Bulgeri Formation.||||
16201|Rockfields Member|68336|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.||Is overlain by Stopem Blockem Conglomerate Member.|Drab, fine- to medium-grained, lithofeldspathic sandstone, mudstone and fine-grained redbeds; minor polymictic conglomerate and green tuff.|
16201|Rockfields Member|68341|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Graveyard Creek Subprovince.||Unit in Bulgeri Formation.||Is overlain by Stopem Blockem Conglomerate Member.|Drab, fine- to medium-grained, lithofeldspathic sandstone, mudstone and fine-grained redbeds; minor polymictic conglomerate and green tuff.|
16201|Rockfields Member|68478|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Basal Member of the Bulgeri Formation.|||Drab, fine to medium-grained, lithofeldspathic sandstone, mudstone and fine-grained redbeds; minor polymictic conglomerate and green tuff.|
16201|Rockfields Member|68479|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Bundock Basin.||Basal Member of the Bulgeri Formation.||Shown as older than the Stopem Blockem Conglomerate Member.|Drab, fine to medium-grained, lithofeldspathic sandstone, mudstone and fine-grained redbeds; minor polymictic conglomerate and green tuff.|
16201|Rockfields Member|69592|5|Briefly described|p259, p273, p298|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. Up to 800m thick; widely distributed. Pervasive soft-sediment deformation, thought to be seismically induced, is distinctive.||Bulgeri Formation.||Unconformably overlies Mytton Formation (Broken River Group). Is overlain by Turrets Formation.|Basal polymict, pebble to cobble conglomerate (up to 25m thick), overlain by well-sorted, fine- to medium-grained sandstone with subordinate siltstone; silicified volcaniclastic siltstone, fine-grained sandstone and red beds occur throughout.|
16202|Rockhampton Group|22482|6|Mentioned|Fig.1|||||||||
16202|Rockhampton Group|22800|6|Mentioned|Fig.14 p592|||||||||
16202|Rockhampton Group|23468|4|Described|p 305|||also see Fig 2 p 295||||||
16202|Rockhampton Group|23799|3|Fully described|p27, p15 Tb. 1|Carboniferous|Devonian|Formerly mapped as Caswell Cr. Gp. and Derrangabungy beds in the MONTO/MUNDUBBERA areas (Murphy, 1976a) - redefined by Yarrol Project Team (1997).  Detailed history of naming of units included on p27.  Max. thickness: <1000m.  Geol. Prov: Yarrol Province.||||||14-DEC-05
16202|Rockhampton Group|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
16202|Rockhampton Group|24399|3|Fully described|p275, p272 Fig. 1|Early Carboniferous|Early Carboniferous|Characterised by thick lenses of oolitic limestone, although not dominant.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt.||||||
16202|Rockhampton Group|24420|4|Described|p7|Early Carboniferous|Early Carboniferous|Previously mapped as Caswell Creek Group.||||||
16202|Rockhampton Group|24467|5|Briefly described|p392|Early Carboniferous|Late Devonian|Geological Province: Yarrol Terrane||||||
16202|Rockhampton Group|24488|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|24489|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|24491|4|Described|p19|Early Carboniferous|Early Carboniferous|Now includes Neils Creek Clastics, Caswell Creek Group and Cania Formation. Formerly referred to as Rockhampton Series.||||||
16202|Rockhampton Group|24571|6|Mentioned|p4|||||||||
16202|Rockhampton Group|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Cr].  Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||
16202|Rockhampton Group|30451|6|Mentioned|p30|||||||||
16202|Rockhampton Group|30840|5|Briefly described|p780|||||||||
16202|Rockhampton Group|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
16202|Rockhampton Group|31519|6|Mentioned|p917|||||||||
16202|Rockhampton Group|31656|6|Mentioned|p6|||||||||
16202|Rockhampton Group|31657|4|Described|p94|||See also p95, 101. U.Tournaisian to U.Visean||||||12-NOV-15
16202|Rockhampton Group|31658|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|31659|4|Described|p51, p52-54|Visean|Tournaisian|max. thickness: 6500ft. Mudstone, siltstone, feldspathic and lithic sandstone, conglomerate, oolitic limestone. See also Table 1.||||||08-OCT-08
16202|Rockhampton Group|32141|6|Mentioned|p149|||Visean||||||
16202|Rockhampton Group|32358|4|Described|Table 2|||p15.||||||12-NOV-15
16202|Rockhampton Group|32959|6|Mentioned|p47|||||||||
16202|Rockhampton Group|33879|6|Mentioned|p284|||||||||
16202|Rockhampton Group|34155|6|Mentioned|p91|||Lower Carboniferous. See also p105.||||||12-NOV-15
16202|Rockhampton Group|34287|6|Mentioned|p110|||See also p111.||||||12-NOV-15
16202|Rockhampton Group|34346|6|Mentioned|p1|||||||||
16202|Rockhampton Group|35008|5|Briefly described|p178|||||||||
16202|Rockhampton Group|35266|6|Mentioned|p201|||||||||
16202|Rockhampton Group|35952|5|Briefly described|p500|||||||||
16202|Rockhampton Group|36210|6|Mentioned|Fig.1|||See also p263.||||||12-NOV-15
16202|Rockhampton Group|36528|6|Mentioned|p173|||||||||
16202|Rockhampton Group|37565|6|Mentioned|Fig.6|||See also Fig.8||||||
16202|Rockhampton Group|38081|5|Briefly described|Table 1|||||||||
16202|Rockhampton Group|38084|5|Briefly described|p54|||||||||
16202|Rockhampton Group|38406|5|Briefly described|p11|||||||||
16202|Rockhampton Group|39445|6|Mentioned|Table 6|||||||||
16202|Rockhampton Group|39973|6|Mentioned|p4|||||||||
16202|Rockhampton Group|39987|6|Mentioned|p65|||||||||
16202|Rockhampton Group|40623|5|Briefly described|p79|||||||||
16202|Rockhampton Group|40735|6|Mentioned|Fig.1|||||||||
16202|Rockhampton Group|41576|4|Described|p17|||See also Table 1.||||||12-NOV-15
16202|Rockhampton Group|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
16202|Rockhampton Group|41826|6|Mentioned|p325|||||||||
16202|Rockhampton Group|41922|4|Described|Table 1, p10|||||||||12-NOV-15
16202|Rockhampton Group|41925|5|Briefly described|p44|||||||||
16202|Rockhampton Group|42486|5|Briefly described|p198|||||||||
16202|Rockhampton Group|42547|5|Briefly described|p49|||||||||
16202|Rockhampton Group|42583|5|Briefly described|p65|||||||||
16202|Rockhampton Group|42929|5|Briefly described|p458|||||||||
16202|Rockhampton Group|43771|5|Briefly described|p813||Early Carboniferous|||||||
16202|Rockhampton Group|44091|14|Not recorded|p36||Early Carboniferous|||||||
16202|Rockhampton Group|44360|14|Not recorded|p4,31||Early Carboniferous|Compared with Caswell Creek Group. See also Lexicon.||||||
16202|Rockhampton Group|44369|2|Defined|p174-175|||See also Lexicon.||||||
16202|Rockhampton Group|44370|14|Not recorded|p219,Tb.7|||See also Lexicon.||||||
16202|Rockhampton Group|44379|14|Not recorded|p15|||Ref. to Fleming 1967.||||||
16202|Rockhampton Group|44388|2|Defined|p113,116||Early Carboniferous|Includes Gudman Oolite, Malchi Formation, Lion Creek Limestone.||||||
16202|Rockhampton Group|44619|14|Not recorded|Fig.2,p189,190|Visean|Tournaisian|(Tournaisian-Early Visean)||||||
16202|Rockhampton Group|44852|14|Not recorded|p73||Early Carboniferous|||||||
16202|Rockhampton Group|45097|6|Mentioned|p23|||?Correlation with Cania Fm.||||||
16202|Rockhampton Group|48921|6|Mentioned|p10|||||||||
16202|Rockhampton Group|50197|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50207|5|Briefly described|Map Legend|Early Permian|Early Carboniferous|||||||
16202|Rockhampton Group|50208|5|Briefly described|Map Legend|Early Permian|Early Carboniferous|||||||14-MAY-04
16202|Rockhampton Group|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Includes: Gudman Oolite, Malchi Formation, Lion Creek Limestone.||||||
16202|Rockhampton Group|50212|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50213|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Overlain by Lorray Formation.||||||17-MAY-04
16202|Rockhampton Group|50214|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Overlain by  Youlambie Conglomerate.||||||17-MAY-04
16202|Rockhampton Group|50317|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50598|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate.||||||21-JUL-04
16202|Rockhampton Group|60282|5|Briefly described|p9|Early Carboniferous|Early Carboniferous|Geological Province: Yarrol Province.||||||
16202|Rockhampton Group|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid bearing sandstone and conglomerate with mudstone rip up clasts; limestone; rare rhyolitic ignimbrite.||||||
16202|Rockhampton Group|60557|4|Described|p18 Fig. 5a, p22|Carboniferous|Carboniferous|Conformably overlies the Mount Alma Formation; conformably to disconformably overlain by Lorray Formation.  See also p19-20 Figs. 5b,c and p39.||||||09-JUN-05
16202|Rockhampton Group|60705|5|Briefly described|p645, p655|Early Carboniferous|Early Carboniferous|Correlative of the Campwyn Volcanics in northern New England Fold Belt. Age: 385-321 Ma and 350.9+/-2.7 Ma as the crystalline age. Geological Province: Yarrol terrane.||||||12-APR-05
16202|Rockhampton Group|61035|5|Briefly described|p13|Carboniferous|Early Carboniferous|Includes; Tournaisian oolitic limestones, Campwyn Volcanics. Geological Province: Yarrol Province.||||||07-FEB-11
16202|Rockhampton Group|61557|5|Briefly described|p878.|||Yarrol Shelf. Crops out SW of Rockhampton. ~2000m thick sequence deposited on a tectonically and volcanically active marine shelf bordering a continental landmass to the west.|||Includes Gudman Formation.||Sequence of siliciclastic-volcaniclastic sedimentary rocks punctuated by minor, scattered, laterally discontinuous carbonate intervals.|
16202|Rockhampton Group|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Early Carboniferous|Geological Province: Yarrol Province. See also p1000 Fig.3, p1008.||||||
16202|Rockhampton Group|61777|5|Briefly described|p230|||Geological Province: Yarrol Province.||||||07-FEB-11
16202|Rockhampton Group|61778|5|Briefly described|p234 Fig. 1, p237|Early Carboniferous|Early Carboniferous|Geological Province: Berserker Subprovince.||||||07-FEB-11
16202|Rockhampton Group|63832|6|Mentioned|p131 fig 2|Carboniferous|Carboniferous|Of east Bowen Basin.||||||
16202|Rockhampton Group|64398|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Dark grey mudstone, siltstone, felsic volcanoclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||18-AUG-08
16202|Rockhampton Group|64399|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Overlain by Lorray Fm. Dk grey mudst, siltst., felsic volcaniclastic sandst., polymictic conglom., ooid-bearing sandstone + conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||19-AUG-08
16202|Rockhampton Group|64429|6|Mentioned|p16 Fig.1|Early Carboniferous|Early Carboniferous|Part of the Yarrol Block.||||||
16202|Rockhampton Group|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Carboniferous|Northern New England Fold Belt. Shown with Campwyn Volcanics. Biostratigraphic age control for top and oolitic limestone intervals. Also some radiometric age control within Group.||||||
16202|Rockhampton Group|65003|5|Briefly described|p3, p19|Early Carboniferous|Early Carboniferous|Of Yarrol Province. Sedimentary and volcanic rocks.||||||30-MAR-12
16202|Rockhampton Group|65388|4|Described|p73-74; p70, 58, 69, p70, 208, 439|Tournaisian||Rockhampton Subprovince, Yarrol Province. Previously unnamed D-Ca unit of Malone, 1970; Studied on the western side of Long Island by Leitch and others (1994) and were assigned to the Campwyn Volcanics; overlain conformably (gradationally) by rocks assigned to the Lorray Formation.  Unconformably overlain by Muncon Volcanics. Age: 350.9+/- 2.7 Ma U-Pb LA-ICP-MS age (Bryan et al 2004). Volcaniclastics and oolitic limestone (towards top).||||||
16202|Rockhampton Group|67203|5|Briefly described|p7, p10-11, p30-31|Early Carboniferous|Early Carboniferous|Formed a topographically diverse basement to Bobby Volcanics.||||Is overlain unconformably by Bobby Volcanics.||
16202|Rockhampton Group|67874|5|Briefly described|p14-15|Carboniferous|Carboniferous|||||Is overlain unconformably by Bobby Volcanics.||06-NOV-15
16202|Rockhampton Group|68008|2|Defined|Throughout.|Visean|Tournaisian|See also. Fleming (1960, 1967). Originally the Rockhampton Series of Daintree (1870). Expanded by the Yarrol Project Team (1997) to include the former Caswell Creek Group, Neils Creek Clastics, Cannindah Limestone and Cania Formation. Thus it is the most widely distributed unit in Yarrol Province: a discontinuous belt of scattered outcrops 260km long and up to 55km wide. The type sections for each constituent are in the type area at Malchi Creek (Fleming, 1967); details given of changes to the upper boundary (Lion Creek Limestone). 1980m thick at type section; up to c.4000m elsewhere. In Glenmore and Yarwun areas, mapped areas of the Group have been reassigned to Mount Alma Formation and Berserker Group respectively. Eleven sedimentary facies and six facies associations are described in great detail. Oolitic limestone is identical in lithology and age to that in Balaclava Formation. Geochemistry described in some detail. Geophysics modelling. Extremely low magnetic response. Numerous zircon U-Pb ages from ignimbrites; also 356.8+/-3.8 Ma (Fanning, 2012). Princhester Serpentinite is thrust over this unit. Structure and its timing discussed. Micropaleontology detailed. Shelly fossils listed; locations. Measured section diagram.|361.1 +/- 5.2 Ma; 350.9 +/- 2.7 Ma.||Gudman Oolite, Malchi Formation, Lion Creek Limestone.|Overlies Balaclava Formation, Three Moon Conglomerate and Mount Alma Formation. Is overlain by Lorray Formation and many others. Numerous intrusions. Equivalent to Wandilla Formation.|Dominated by siltstone and mudstone. Also calcareous sandstones, feldspatholithic sandstones, polymictic conglomerate, and characteristic oolitic/pisolithic limestones and ooid-bearing sandstones. Local andesitic to rhyolitic lavas and pyroclastics.|
16202|Rockhampton Group|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Yarrol Province.||||||
16202|Rockhampton Group|68679|4|Described|p308, p312-314, p316-317, p321, p337-341|Mississippian|Mississippian|See also p345, p347, p349-350, p419, p425-426, p441, p443 Fig.5.103, p468. Fleming (1960, 1967) in the Neerkol area. Rockhampton Subprovince, Northern Yarrol Province. Mainly volcaniclastic sediments from an arc to the west, but is characterised by repeated development of oolitic carbonate banks along the W margin. Lithologies and fossil faunas described in some detail. A source of sediments for the Moah Creek beds. U-Pb zircon ages by Bryan et al. (2004). RELATED UNITS (continued):  Is intruded by May Queen, Gracemere Gabbros, Zig Zag Tonalite, Mannersley Quartz Microdiorite, Bajool Quartz Diorite, Kabra Quartz Monzodiorite, Pack Granite and Bocoolima, Rocky Point Granodiorites.|361.1 +/- 5.2 Ma; 350.9 +/- 2.7 Ma.||Gudman Ooloite, Malchi Formation, Lion Creek Limestone.|Is overlain by Lorray Formation and unconformably by Berserker Group and Bobby Volcanics. Is faulted against the Marble Waterhole beds. See COMMENTS for more.|Oolitic, bioclastic and pisolitic limestone; calcareous, ooid-rich, medium to coarse sandstone; calcareous, fossiliferous, fine-grained to very coarse-grained sandstone; ooid-bearing feldspatholithic sandstone; siltstone and mudstone; conglomerate.|
16202|Rockhampton Group|69594|6|Mentioned|p561|||||||Is intruded by Ridler Monzonite.||
16202|Rockhampton Group|69952|6|Mentioned|p75|Early Carboniferous|Early Carboniferous|||||||06-NOV-15
16202|Rockhampton Group|70050|5|Briefly described|p316|Early Carboniferous|Early Carboniferous|Yarrol Basin. The type area is in the Lion Creek, Ridgelands and Fitzroy blocks. Numerous (coral) fossiliferous locality investigations mentioned.||||||
16202|Rockhampton Group|73197|6|Mentioned|p467|Carboniferous|Early Carboniferous|New England Orogen, northern. Yarrol Province. Forearc basin shallow marine environment. Described as lower to mid Carboniferous in text.|||||Common oolitic limestones.|
16202|Rockhampton Group|73450|6|Mentioned|p36, p59, p67|Carboniferous|Carboniferous|||||Intruded by Toondahra Granite and Ridler Monzonite (Glassford Igneous Complex).||
16216|Rocksberg Greenstone|22784|6|Mentioned|p3|||||||||
16216|Rocksberg Greenstone|22845|4|Described|p7,9-12,67,fig6|||After Bryan an Jones (1950) and Cranfield (1976).  Correlates with Peters Creek Greenstone.||||||
16216|Rocksberg Greenstone|22846|6|Mentioned|p44|Carboniferous|Devonian|Intruded by Neurum Complex.||||||
16216|Rocksberg Greenstone|23251|6|Mentioned|p3|||Was previously included in the Gympie Group by Day & others (1978). Gympie Group.||||||
16216|Rocksberg Greenstone|23542|5|Briefly described|Fig 1 p378|||||||||
16216|Rocksberg Greenstone|24418|5|Briefly described|p5, Map 1|Carboniferous|Carboniferous|Volcanic rocks of basaltic composition. Strongly deformed. Outcrop: pale green, strong foliation (layering), fine grained greenschist, some layers mica schist.||||||30-JUN-06
16216|Rocksberg Greenstone|29555|6|Mentioned|p12|||||||||
16216|Rocksberg Greenstone|30797|5|Briefly described|Table 1|||Palaeozoic, useful for concrete aggregate and road screenings.||||||
16216|Rocksberg Greenstone|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
16216|Rocksberg Greenstone|30915|6|Mentioned|p101|||||||||
16216|Rocksberg Greenstone|31131|5|Briefly described|p153|||Contact with Neranleigh-Fernvale Gp. discussed.||||||
16216|Rocksberg Greenstone|31271|6|Mentioned|Fig. 2|||||||||
16216|Rocksberg Greenstone|31756|6|Mentioned|p16|||Early Palaeozoic||||||
16216|Rocksberg Greenstone|31757|6|Mentioned|p9|||||||||
16216|Rocksberg Greenstone|31811|6|Mentioned|Fig. 1|||||||||
16216|Rocksberg Greenstone|31999|6|Mentioned|p133|||||||||
16216|Rocksberg Greenstone|35007|6|Mentioned|p73|||||||||
16216|Rocksberg Greenstone|35101|3|Fully described|p11|||||||||
16216|Rocksberg Greenstone|35126|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16216|Rocksberg Greenstone|35156|5|Briefly described|p4|||See also Table.2||||||
16216|Rocksberg Greenstone|35410|6|Mentioned|p91|||||||||
16216|Rocksberg Greenstone|35430|6|Mentioned|Table 1|||Interpretation of stratigraphic successions||||||
16216|Rocksberg Greenstone|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
16216|Rocksberg Greenstone|35866|6|Mentioned|p400|||See also P402.||||||
16216|Rocksberg Greenstone|36238|6|Mentioned|Table 1|||||||||
16216|Rocksberg Greenstone|36440|6|Mentioned|Map legend|Late Carboniferous|Early Carboniferous|Early to Late Carboniferous||||||
16216|Rocksberg Greenstone|36528|6|Mentioned|p171|||Also mention P174.||||||
16216|Rocksberg Greenstone|36547|6|Mentioned|Table 2|||||||||
16216|Rocksberg Greenstone|37252|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16216|Rocksberg Greenstone|38074|5|Briefly described|Table 1|||||||||
16216|Rocksberg Greenstone|38077|5|Briefly described|p29|||||||||
16216|Rocksberg Greenstone|38391|6|Mentioned|p7|||||||||
16216|Rocksberg Greenstone|39079|5|Briefly described|p6|||||||||
16216|Rocksberg Greenstone|39445|5|Briefly described|Table 7|||See also P79, P83 & Fig.7||||||
16216|Rocksberg Greenstone|40051|4|Described|p5|||||||||
16216|Rocksberg Greenstone|40245|6|Mentioned|p182|||||||||
16216|Rocksberg Greenstone|40475|6|Mentioned|p3|||||||||
16216|Rocksberg Greenstone|40517|6|Mentioned|p358|||||||||
16216|Rocksberg Greenstone|40579|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
16216|Rocksberg Greenstone|40623|5|Briefly described|p53|||||||||
16216|Rocksberg Greenstone|41917|6|Mentioned|p521|||||||||
16216|Rocksberg Greenstone|42525|5|Briefly described|Map legend|Paleozoic|Paleozoic|Geological Province: D'Aguilar Block.||||||07-NOV-08
16216|Rocksberg Greenstone|42547|4|Described|p54, p55|||||||||
16216|Rocksberg Greenstone|42619|6|Mentioned|p29|||||||||
16216|Rocksberg Greenstone|42970|5|Briefly described|p117|||||||||
16216|Rocksberg Greenstone|43006|5|Briefly described|Table 1,p239|||||||||
16216|Rocksberg Greenstone|43017|5|Briefly described|p379|||||||||
16216|Rocksberg Greenstone|43076|5|Briefly described|p5|||||||||
16216|Rocksberg Greenstone|43092|5|Briefly described|Fig.2|||||||||
16216|Rocksberg Greenstone|43100|6|Mentioned|p6|||||||||
16216|Rocksberg Greenstone|44211|14|Not recorded|p89|||||||||
16216|Rocksberg Greenstone|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
16216|Rocksberg Greenstone|45003|14|Not recorded|p256|||||||||
16216|Rocksberg Greenstone|48940|5|Briefly described|p7|||Refers Bryan & Jones (1950), Mathews (1954)||||||
16216|Rocksberg Greenstone|60077|5|Briefly described|Map legend|Paleozoic|Paleozoic|Basic metavolcanics.||||||07-NOV-08
16216|Rocksberg Greenstone|68327|5|Briefly described|Map legend.|Paleozoic|Paleozoic||||||Greenstone.|
16216|Rocksberg Greenstone|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek Greenstone, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
16216|Rocksberg Greenstone|68679|5|Briefly described|p321, p324, p326-329, p332, p369|||Northern New England Orogen. Forms a narrow NNW-trending belt east of Dayboro. Detachment zone and lower plate accretionary assemblages; may represent subducted seamount material exhumed during later extension. Typical of equivalent units such as Peters Creek Greenstone (a correlate) and parts of the Widgee and Wongella Metamorphics. Tectonically interleaved with Kurwongah beds. Thermochronology of phengite ages by Little, Holcombe abd McWilliams (1993).|~262-260 Ma : 40Ar/39Ar plateau ages.|||Is overlain unconformably by Mount Byron Volcanics. Is intruded by Neurum Complex. Is faulted against Jimna Phyllite, Northbrook beds and Neara Volcanics. Correlated with Mount Mia Serpentinite.|Strongly foliated, moderately to coarsely crystalline greenschist containing discrete layers millimetres to metres thick, with blue amphibole; highly deformed fragmental rocks common; blueschist-greenschist units with abundant pseudomorphs after cpx.|
16262|Rolleston Conglomerate|36103|6|Mentioned|p146|||||||||
16262|Rolleston Conglomerate|48900|6|Mentioned|Table 3|||||||||
16262|Rolleston Conglomerate|63713|5|Briefly described|p1508|||Denison Trough, Bowen Basin.||||Is overlain by Reids Dome Beds.||
16267|Rolling Downs Group|730|6|Mentioned|p24, p25.|||Marine.||||||11-NOV-14
16267|Rolling Downs Group|9250|5|Briefly described|Map legend|Cretaceous|Cretaceous|Sandstone, siltstone and claystone., porcellaneous in part.||||||
16267|Rolling Downs Group|12575|5|Briefly described|p781. |Albian|Albian|Uppermost unit in Laura Basin. Vitrinite reflectance data are detailed.|124-97 Ma.||Includes Wollena Claystone.||Glauconitic open marine shale.|
16267|Rolling Downs Group|13516|5|Briefly described|p167 fig 10, p169 fig 11|Late Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.|||Includes Wilgunya Subgroup, Manuka Subgroup|||14-NOV-12
16267|Rolling Downs Group|22757|5|Briefly described|p7|||Also Table6, p11. Surat Basin.||||||28-NOV-06
16267|Rolling Downs Group|22780|5|Briefly described|map|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|22781|4|Described|p41|Early Cretaceous|Early Cretaceous|In the Carpentaria Basin.||||||02-APR-07
16267|Rolling Downs Group|22857|5|Briefly described|p294, p544 App.1 Tb.A1.12|Cenomanian|Aptian|Includes the Wallumbilla Formation, Surat Siltstone, Griman Creek Formation, and Winton Formation. Geological Province: Surat and Eromanga Basins. See also p296-7 Tb.22.1, p315 Fig. 22.8, p552 App.1 Tb.A1.13.||||||
16267|Rolling Downs Group|22865|4|Described|p294,Table22.1p296-7|Cenomanian|Aptian|||||||
16267|Rolling Downs Group|23053|4|Described|p8,11,28,30-1|Albian|Aptian|||||||
16267|Rolling Downs Group|23056|6|Mentioned|6|||Geological province: Eromanga Basin.||||||28-NOV-06
16267|Rolling Downs Group|23065|5|Briefly described|18|||Geological province: Carpentaria Basin.||||||28-NOV-06
16267|Rolling Downs Group|23183|6|Mentioned|p217||Aptian|||||||
16267|Rolling Downs Group|23220|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|23224|5|Briefly described|p3|||Of McMinn 1981. Hosts the Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
16267|Rolling Downs Group|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Coffin Hill Member. Thickness: <10m. Geological Province: Georgetown Region.||||||26-NOV-08
16267|Rolling Downs Group|23336|5|Briefly described|p5|Cretaceous|Cretaceous|Overlies Mulga Downs Group.||||||28-NOV-06
16267|Rolling Downs Group|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23420|6|Mentioned|p 131|||||||||
16267|Rolling Downs Group|23423|5|Briefly described|p267||Cretaceous|||||||
16267|Rolling Downs Group|23425|3|Fully described|p394 Table 9.7.|||Also see p378. Geological Province Carpentaria Basin.||||||03-APR-12
16267|Rolling Downs Group|23426|3|Fully described|p403 + Table 10.4 p407|Albian|Aptian|Formerly Battle Camp Shale and Wolena Claystone. Conformably underlain by Gilbert River Formation. Geological province: Laura Basin Province.||||||26-APR-07
16267|Rolling Downs Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
16267|Rolling Downs Group|23428|5|Briefly described|p422|||||||||
16267|Rolling Downs Group|23430|5|Briefly described|p522|||Formerly Battle Camp Shale and Wolena Claystone. Basal shale is marine, variably calcareous and galuconitic, with minor siltstone and conglom. beds; overlain by marine silty/sandy claystone with calc.concretions. Geol. Prov: Laura Basin.||||||30-NOV-06
16267|Rolling Downs Group|23431|5|Briefly described|p544|||||||||
16267|Rolling Downs Group|23496|6|Mentioned|p59|||||||||
16267|Rolling Downs Group|23510|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|23833|5|Briefly described|p256 Table 1|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23879|6|Mentioned|p18|||||||||
16267|Rolling Downs Group|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
16267|Rolling Downs Group|23911|5|Briefly described|p97 Fig. 11|Albian|Aptian|Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|23982|5|Briefly described|p2|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
16267|Rolling Downs Group|24047|5|Briefly described|p11-12|||Geological Province: Western Gulf Sub-basin.||||||
16267|Rolling Downs Group|24048|6|Mentioned|p76|||Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
16267|Rolling Downs Group|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24089|5|Briefly described|Student Activites|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Shallow marine deposits <50m. thick.||||||
16267|Rolling Downs Group|29591|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|29961|6|Mentioned|p12|||||||||
16267|Rolling Downs Group|29991|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30019|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|30021|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30102|5|Briefly described|p34|||Cretaceous age. See also p17.||||||28-NOV-06
16267|Rolling Downs Group|30103|5|Briefly described|p9|||Lower Cretaceous age. Table 3 on p9. See also Fig.2.||||||28-NOV-06
16267|Rolling Downs Group|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30133|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30510|6|Mentioned|p103|||||||||
16267|Rolling Downs Group|30582|6|Mentioned|p4|||||||||
16267|Rolling Downs Group|30584|4|Described|Table 1|||||||||
16267|Rolling Downs Group|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30691|4|Described|p6|||See also p15-17,20,Table 4,Fig.2. Lower Cretaceous age.||||||28-NOV-06
16267|Rolling Downs Group|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30696|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|30697|6|Mentioned|p34|||Minor aquifer present.||||||28-NOV-06
16267|Rolling Downs Group|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous||||||
16267|Rolling Downs Group|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30702|4|Described|p48|||See also p51,52,Fig.1. Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|30853|5|Briefly described|Table 3|||Cretaceous||||||
16267|Rolling Downs Group|30854|4|Described|Table 4|||Lower to Upper Cretaceous age||||||
16267|Rolling Downs Group|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30856|4|Described|Table 3|||Lower Cretaceous age||||||
16267|Rolling Downs Group|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30905|6|Mentioned|p147|||||||||
16267|Rolling Downs Group|30910|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31098|5|Briefly described|Table 1|||||||||
16267|Rolling Downs Group|31109|6|Mentioned|p40|||See also P42, 44, 46, 50, 52, 54, 56, 58 & Map 62.||||||
16267|Rolling Downs Group|31110|5|Briefly described|p6|||See also p8-26. Terrain classification.||||||28-NOV-06
16267|Rolling Downs Group|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
16267|Rolling Downs Group|31164|6|Mentioned|p8|||Lower Cretaceous||||||
16267|Rolling Downs Group|31165|5|Briefly described|Table.1.|||||||||
16267|Rolling Downs Group|31166|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31376|5|Briefly described|p4|||Mention p2.||||||28-NOV-06
16267|Rolling Downs Group|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes the Wallumbilla Formation, Toolebuc Limestone and Allaru Mudstone.||||||02-DEC-04
16267|Rolling Downs Group|31425|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31430|4|Described|Table 1|||||||||
16267|Rolling Downs Group|31431|5|Briefly described|Table 3|||L.U.Cretaceous||||||
16267|Rolling Downs Group|31432|4|Described|Table 1|||L.Cretaceous||||||
16267|Rolling Downs Group|31433|5|Briefly described|p7|||Lower Cretaceous||||||
16267|Rolling Downs Group|31434|4|Described|Table 1|||Lower Cretaceous. See also p8.||||||28-NOV-06
16267|Rolling Downs Group|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous||||||
16267|Rolling Downs Group|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32274|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32275|4|Described|p8|||||||||
16267|Rolling Downs Group|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32277|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32314|6|Mentioned|Fig.4|||||||||
16267|Rolling Downs Group|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32395|6|Mentioned|p6|||Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|32396|6|Mentioned|p8|||L.Cretaceous||||||
16267|Rolling Downs Group|32413|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|32563|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|32705|6|Mentioned|p183|||See also Fig.2||||||
16267|Rolling Downs Group|32706|4|Described|Table 1|||Mention p8.||||||28-NOV-06
16267|Rolling Downs Group|32796|4|Described|p301|||See also p302-303||||||28-NOV-06
16267|Rolling Downs Group|32918|4|Described|p18|||||||||11-JAN-10
16267|Rolling Downs Group|33011|6|Mentioned|p214|||||||||
16267|Rolling Downs Group|33016|6|Mentioned|p1|||||||||
16267|Rolling Downs Group|33017|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Includes Winton, Mackunda and Wallumbilla Formations and Allaru Mudstone and Toolebuc Limestone.||||||07-JUL-04
16267|Rolling Downs Group|33068|6|Mentioned|p476|||Cret.||||||
16267|Rolling Downs Group|33069|4|Described|p7|||L.-U.Cret.||||||
16267|Rolling Downs Group|33070|4|Described|Table 2|||L.Cret.||||||
16267|Rolling Downs Group|33072|4|Described|Table 1|||L.Cret.||||||
16267|Rolling Downs Group|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33075|6|Mentioned|p452|||||||||
16267|Rolling Downs Group|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33087|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33088|4|Described|Table 3|||L.Cret.||||||
16267|Rolling Downs Group|33089|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33090|4|Described|Table 4|||L.Cret.||||||
16267|Rolling Downs Group|33091|6|Mentioned|p9|||Strat.||||||
16267|Rolling Downs Group|33092|6|Mentioned|p8|||Strat. table||||||
16267|Rolling Downs Group|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33150|4|Described|p8|||L.Cret.||||||
16267|Rolling Downs Group|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33176|6|Mentioned|p175|||||||||
16267|Rolling Downs Group|33177|5|Briefly described|Table 1|||||||||15-JUL-04
16267|Rolling Downs Group|33178|5|Briefly described|p11|||||||||
16267|Rolling Downs Group|33181|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33182|6|Mentioned|p193|||||||||
16267|Rolling Downs Group|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33226|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33372|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
16267|Rolling Downs Group|33449|4|Described|Table 1|||L.-U.Cret.||||||
16267|Rolling Downs Group|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33529|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33561|6|Mentioned|p102|||||||||
16267|Rolling Downs Group|33638|5|Briefly described|Table 1|||See also p10.||||||28-NOV-06
16267|Rolling Downs Group|33639|5|Briefly described|p11|||L.Cret.||||||
16267|Rolling Downs Group|33640|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33642|6|Mentioned|p144,147,148|||Refers Vine & Day.(1965). Ref. to Whitehouse 1954. Subgroups. Ref to Jack 1886.||||||
16267|Rolling Downs Group|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33646|5|Briefly described|p8|||Strat. table.||||||
16267|Rolling Downs Group|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
16267|Rolling Downs Group|33648|6|Mentioned|p19|||||||||
16267|Rolling Downs Group|33676|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33709|6|Mentioned|p110|||Cretaceous.||||||
16267|Rolling Downs Group|33772|4|Described|p13|||||||||
16267|Rolling Downs Group|33773|4|Described|Table 1|||||||||
16267|Rolling Downs Group|33825|6|Mentioned|p10|||Correlation table||||||
16267|Rolling Downs Group|33832|5|Briefly described|p11|||Strat. and correlation.||||||28-NOV-06
16267|Rolling Downs Group|33882|4|Described|Table 1|||Mention p7,8.||||||28-NOV-06
16267|Rolling Downs Group|33883|6|Mentioned|p17|||||||||
16267|Rolling Downs Group|33884|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34065|4|Described|p6|||L.Cret.||||||
16267|Rolling Downs Group|34091|5|Briefly described|Table 1|||Cret. See also pp4,8.||||||28-NOV-06
16267|Rolling Downs Group|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
16267|Rolling Downs Group|34218|5|Briefly described|Table 1|||Lower Cretaceous.||||||28-NOV-06
16267|Rolling Downs Group|34254|6|Mentioned|p481|||||||||
16267|Rolling Downs Group|34282|6|Mentioned|p96|||Cret.||||||
16267|Rolling Downs Group|34287|6|Mentioned|p186|||Cret.||||||
16267|Rolling Downs Group|34469|6|Mentioned|p107|||Cretaceous. See also pp117,118.||||||28-NOV-06
16267|Rolling Downs Group|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34550|5|Briefly described|Table 2.1|||Cretaceous||||||
16267|Rolling Downs Group|34811|4|Described|Table 1|||||||||
16267|Rolling Downs Group|34931|5|Briefly described|p320|||||||||
16267|Rolling Downs Group|35187|6|Mentioned|p53|||||||||
16267|Rolling Downs Group|35204|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35220|4|Described|p16|||||||||
16267|Rolling Downs Group|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35559|4|Described|Table 1|||||||||
16267|Rolling Downs Group|35560|6|Mentioned|p289|||||||||
16267|Rolling Downs Group|35601|6|Mentioned|p144|||Geothermal gradients correlate with contours of base of R.D.Group||||||
16267|Rolling Downs Group|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35663|6|Mentioned|Table 1|||Biostratigraphy.||||||
16267|Rolling Downs Group|35793|6|Mentioned|p241|||Weathered profiles.||||||
16267|Rolling Downs Group|35811|5|Briefly described|Table 3|||||||||
16267|Rolling Downs Group|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
16267|Rolling Downs Group|36012|3|Fully described|Table 5|||||||||
16267|Rolling Downs Group|36056|6|Mentioned|p11|||||||||
16267|Rolling Downs Group|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36473|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|36570|6|Mentioned|p46|||||||||
16267|Rolling Downs Group|36571|6|Mentioned|Table 4|||||||||
16267|Rolling Downs Group|36751|6|Mentioned|p488|||||||||
16267|Rolling Downs Group|36910|6|Mentioned|p61|||||||||
16267|Rolling Downs Group|36914|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|36961|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|37116|6|Mentioned|p310|||||||||
16267|Rolling Downs Group|37608|3|Fully described|Table 1|||See also Table 2||||||
16267|Rolling Downs Group|37995|4|Described|Table 1|||||||||
16267|Rolling Downs Group|38064|5|Briefly described|p42|||Contain opal deposits of White Cliffs and Lightning Ridge.||||||
16267|Rolling Downs Group|38226|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|38374|6|Mentioned|p602|||||||||
16267|Rolling Downs Group|39211|6|Mentioned|p5|||Fig. 3,7,9,22,26 etc. Correlation||||||
16267|Rolling Downs Group|39315|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39445|5|Briefly described|Table 11|||||||||
16267|Rolling Downs Group|39478|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|39494|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39627|6|Mentioned|p269|||||||||
16267|Rolling Downs Group|39666|6|Mentioned|p110|||||||||
16267|Rolling Downs Group|39708|6|Mentioned|p478|||||||||
16267|Rolling Downs Group|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39942|6|Mentioned|p468|||||||||
16267|Rolling Downs Group|40030|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|40199|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|40544|6|Mentioned|Fig.6|||||||||
16267|Rolling Downs Group|40584|6|Mentioned|p434|||||||||
16267|Rolling Downs Group|40595|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|40623|5|Briefly described|p88|||||||||
16267|Rolling Downs Group|40648|3|Fully described|p12|||||||||
16267|Rolling Downs Group|40766|5|Briefly described|p25|||||||||
16267|Rolling Downs Group|40801|6|Mentioned|p79|||||||||
16267|Rolling Downs Group|40926|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|41012|6|Mentioned|p137|||||||||
16267|Rolling Downs Group|41022|6|Mentioned|p279|||||||||
16267|Rolling Downs Group|41061|6|Mentioned|p19|||See also Fig.6. Generalized stratigraphy.||||||28-NOV-06
16267|Rolling Downs Group|41064|6|Mentioned|p55|||||||||
16267|Rolling Downs Group|41086|3|Fully described|p98|||See also Fig.3||||||
16267|Rolling Downs Group|41087|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41088|6|Mentioned|p143|||||||||
16267|Rolling Downs Group|41097|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|41117|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41177|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41188|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41210|5|Briefly described|Fig.3|||||||||
16267|Rolling Downs Group|41247|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|41266|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41307|4|Described|p17|||||||||
16267|Rolling Downs Group|41568|4|Described|p15|||||||||
16267|Rolling Downs Group|41642|6|Mentioned|p217|||||||||
16267|Rolling Downs Group|41681|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|41725|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41992|4|Described|Fig.2 P183|||See also p186.||||||28-NOV-06
16267|Rolling Downs Group|42007|6|Mentioned|Fig.2 P182|||||||||
16267|Rolling Downs Group|42061|5|Briefly described|Fig.4 P151|||||||||
16267|Rolling Downs Group|42121|6|Mentioned|Fig.1 P97|||||||||
16267|Rolling Downs Group|42346|4|Described|p81, Fig.4 p82|Early Cretaceous||||||||
16267|Rolling Downs Group|42364|5|Briefly described|Fig. 1 P196|||||||||
16267|Rolling Downs Group|42460|5|Briefly described|Fig.1 P206|||||||||
16267|Rolling Downs Group|42464|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|42467|5|Briefly described|Map Legend|||||||||
16267|Rolling Downs Group|42596|5|Briefly described|Fig. 1 P24|||||||||
16267|Rolling Downs Group|42637|5|Briefly described|p10, 23|||||||||
16267|Rolling Downs Group|42650|4|Described|p16|||Conformably overlies/overlaps the Gilbert River Formation.||||||28-NOV-06
16267|Rolling Downs Group|42653|5|Briefly described|p318|||Terrain pattern description||||||
16267|Rolling Downs Group|42673|6|Mentioned|p195|||||||||
16267|Rolling Downs Group|43000|5|Briefly described|Fig.5,p112|||||||||
16267|Rolling Downs Group|43085|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|43090|5|Briefly described|Map legend||Cretaceous|||||||
16267|Rolling Downs Group|43276|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43277|5|Briefly described|Map Legend||Early Cretaceous|In the Great Australian Basin.||||||28-NOV-06
16267|Rolling Downs Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
16267|Rolling Downs Group|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43368|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43369|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43371|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43383|14|Not recorded|p26-28, diag||Cretaceous|||||||
16267|Rolling Downs Group|43384|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43386|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43390|14|Not recorded|p15,16,27-34|||Divided into Winton,Tambo,Roma Formations||||||
16267|Rolling Downs Group|43402|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43403|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43404|14|Not recorded|p11-15,20,23-33||Cretaceous|Table p9,Table p11||||||
16267|Rolling Downs Group|43405|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43410|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43411|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43436|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43452|5|Briefly described|Map Legend||Cretaceous|Includes: Roma Formation, Tambo Formation, Winton Formation.||||||14-FEB-05
16267|Rolling Downs Group|43454|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43459|14|Not recorded|p315-6|||||||||
16267|Rolling Downs Group|43487|5|Briefly described|20|||||||||
16267|Rolling Downs Group|43501|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition) Inc. Yalpunga Beds, Oornoo Beds, Wittabrenna Beds||||||
16267|Rolling Downs Group|43542|14|Not recorded|Map Legend||Cretaceous|lithology||||||
16267|Rolling Downs Group|43596|4|Described|p40, p39 Tb. 4|Albian|Aptian|Max. thickness: 600m. Largely comprises mudstone, with beds and lenses of glauconitic, labile, white to buff quartzose fine sandstone; fossiliferous and with  concretionary limestone at base; shallow marine deposits.||||||15-JAN-09
16267|Rolling Downs Group|43602|5|Briefly described|Fig3 p194|||In Surat Basin/Eromanga Basin||||||
16267|Rolling Downs Group|43625|6|Mentioned|p47|||||||||
16267|Rolling Downs Group|43630|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|43714|6|Mentioned|p8||Early Cretaceous|||||||
16267|Rolling Downs Group|43730|5|Briefly described|p24,29|||||||||
16267|Rolling Downs Group|43738|6|Mentioned|p5|||||||||
16267|Rolling Downs Group|43810|6|Mentioned|Fig.4,p209,210||Cretaceous|||||||
16267|Rolling Downs Group|43820|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43881|14|Not recorded|p79,80|Cretaceous|Late Jurassic|See also Lexicon.||||||
16267|Rolling Downs Group|43995|14|Not recorded|Tb.p9,20 Fig.9||Cretaceous|Inc. Roma Formation, Tambo Formation and Winton Formation in the Eromanga Sub-Basin.||||||
16267|Rolling Downs Group|44020|14|Not recorded|p10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44033|14|Not recorded|Tb.1,opp.p4|||||||||
16267|Rolling Downs Group|44034|6|Mentioned|Tb.1,p2|||||||||
16267|Rolling Downs Group|44041|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|44087|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44089|14|Not recorded|Tb.1||Early Cretaceous|||||||
16267|Rolling Downs Group|44091|14|Not recorded|p60||Cretaceous|||||||
16267|Rolling Downs Group|44093|6|Mentioned|p68 (photo)|||Associated with Gum Vale beds.||||||
16267|Rolling Downs Group|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44112|6|Mentioned|p82|||||||||
16267|Rolling Downs Group|44121|14|Not recorded|p8|||||||||
16267|Rolling Downs Group|44122|14|Not recorded|p322|||||||||
16267|Rolling Downs Group|44207|14|Not recorded|p116|||||||||
16267|Rolling Downs Group|44269|14|Not recorded|p16||Cretaceous|||||||
16267|Rolling Downs Group|44291|14|Not recorded|p5|||||||||
16267|Rolling Downs Group|44346|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44375|14|Not recorded|p313|||||||||
16267|Rolling Downs Group|44406|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44408|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44415|14|Not recorded|p22,Fig.2,p23|||||||||
16267|Rolling Downs Group|44417|2|Defined|p417-421|Albian|Aptian|Contains: Winton, Mackunda and Wilgunya Formations. Overlies Gilbert River Formation. Probably Cenomanian.||||||
16267|Rolling Downs Group|44739|14|Not recorded|p19|||||||||
16267|Rolling Downs Group|44740|14|Not recorded|p29,39-42,47,48,52,|||p55,56,77||||||
16267|Rolling Downs Group|44744|14|Not recorded|p106-113|||||||||
16267|Rolling Downs Group|44800|14|Not recorded|p16,22,map||Cretaceous|||||||
16267|Rolling Downs Group|44819|14|Not recorded|p89|Albian|Aptian|Shaley basal formation is Roma Formation.||||||
16267|Rolling Downs Group|44836|14|Not recorded|p5,11,Figs.1-5||Cretaceous|||||||
16267|Rolling Downs Group|44852|14|Not recorded|p78||Early Cretaceous|||||||
16267|Rolling Downs Group|44989|14|Not recorded|p.125,126|||(E54-14).||||||
16267|Rolling Downs Group|45004|14|Not recorded|p.8|||Tb.1.||||||
16267|Rolling Downs Group|45011|14|Not recorded|p18,20|||Whitehouse correlated sediments in Polland Shale with Rolling Downs Group.||||||
16267|Rolling Downs Group|45110|6|Mentioned|p6|||||||||
16267|Rolling Downs Group|45145|3|Fully described|Table 5|||See also p23.||||||31-OCT-06
16267|Rolling Downs Group|46791|4|Described|p44|||Refers Galloway (1967)||||||
16267|Rolling Downs Group|46802|6|Mentioned|p131|||||||||
16267|Rolling Downs Group|46812|5|Briefly described|p241|||||||||
16267|Rolling Downs Group|46854|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|46872|6|Mentioned|p108|||||||||
16267|Rolling Downs Group|46881|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
16267|Rolling Downs Group|46937|6|Mentioned|Fig.10|||||||||
16267|Rolling Downs Group|46939|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|47042|6|Mentioned|p171|||||||||
16267|Rolling Downs Group|47083|5|Briefly described|p20||Mesozoic|Carpentaria Basin.||||||
16267|Rolling Downs Group|48908|14|Not recorded|Tb.1||Cretaceous|||||||
16267|Rolling Downs Group|48920|3|Fully described|p56|||Cretaceous||||||
16267|Rolling Downs Group|48951|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Comprises Wallumbilla and Toolebuc Formations, Allaru Mudstone and Mackunda Formation.  Overlies the Gilbert River Formation.  Geological Province:  Eromanga Basin.||||||
16267|Rolling Downs Group|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Allaru Mudstone, Toolebuc Limestone, and Wallumbilla Formation.||||||
16267|Rolling Downs Group|61312|5|Briefly described|p66, p73|Albian|Aptian|Supersedes "Rolling Downs Formation". Comprises Wallumbilla and Toolebuc Formations, and Allaru Mudstone and Winton Formation. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Includes the Griman Creek Formation, Surat Siltstone and Wallumbilla Formation. Green silty mudstone, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
16267|Rolling Downs Group|61823|5|Briefly described|p118|||Part of a marine transgressive sequence; overlies Gum Vale and Cadna-Owie Formations. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Includes Wallumbilla Formation, Allaru Mudstone and Normanton Formation.  Age: ~114-91Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
16267|Rolling Downs Group|63450|5|Briefly described|p83|Cretaceous|Jurassic|Overlies Hooray Sandstone/Cadna-owie Formation. Marine deposits.||||||07-FEB-11
16267|Rolling Downs Group|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Subaerial scree and slope debris deopsits on fossil hill slopes and valley walls containing dislodged angular blocks of underlying bedrock. Commonly with pebbly sand infill and silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Beach pebble, cobble and boulder deposits formed from white quartzose sandstone. Commonly with silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63793|6|Mentioned|p10.|Cretaceous|Jurassic|Eromanga Basin.||||||
16267|Rolling Downs Group|63979|6|Mentioned|p51-52|||Includes the Wilgunyah Subgroup.||||||07-FEB-11
16267|Rolling Downs Group|64061|6|Mentioned|p66|Cretaceous|Cretaceous|Contains the Griman Creek Formation. Geological Province: Surat Basin.||||||24-APR-08
16267|Rolling Downs Group|64570|5|Briefly described|p858|Early Cretaceous|Early Cretaceous|Volcanogenic sedimentary rocks and are rich in volcanic lithics.||||||22-DEC-08
16267|Rolling Downs Group|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Gilbert River Formation.|Dominantly marine shales and siltstones.|
16267|Rolling Downs Group|64679|5|Briefly described|Map legend|Cretaceous|Cretaceous|Conglomerate (pebbles of rounded white vein quartz and quartzite), quartz sandstone, siltstone and claystone; commonly silicified or ferruginised.||||||27-NOV-08
16267|Rolling Downs Group|64681|5|Briefly described|p2, p3 Fig. 1|Cretaceous|Cretaceous|Geological province: Eromanga Basin. Sandstone, siltstone, claystone.||||||
16267|Rolling Downs Group|64682|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Feldspathic and lithic sandstone, siltstone and mudstone; strongly kaolinised, mottled and ferruginised, locally containes exotic ?drop? boulders.||||||
16267|Rolling Downs Group|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes Hooray Sandstone. Rounded waterworn white vein quartz and quartzite conglomerate, quartzose sandstones, siltstones and claystones deposited on undulating topography in underlying bedrock.||||||
16267|Rolling Downs Group|64820|4|Described|pS9, pS6 Fig. 4|Late Cretaceous|Middle Jurassic|Contains Garroway Sandstone, Gilbert River, Wallumbilla and Toolbeuc Formations, Allaru Mudstone and Normanton Formation. Overlain by Bulimba Formation.||||||
16267|Rolling Downs Group|64821|5|Briefly described|pS18, pS20-21, pS40|Cretaceous|Cretaceous|Discussed in relation to its saprolite zone in the East Weipa and Andoom areas where lenses of weakly lithified sandstone, clay and siltstone dominate. Unconformably overlain by the Bulimba Formation.||||||02-FEB-09
16267|Rolling Downs Group|64822|5|Briefly described|pS88, pS99|||Together with the overlying Bulimba Fm, hosted the development of the Weipa bauxite deposit - composed of a transported blanket of bauxite overlying a lateritic weathering profile. Geol.prov: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
16267|Rolling Downs Group|66529|6|Mentioned|p12 Fig.5|||Eromanga, Carpentaria, Surat Basins and Coonamble Embayment.|||Includes Wallumbilla, Toolebuc, Mackunda, Winton, Griman Creek Formations; Surat Siltstone; and Allaru Mudstone.|||
16267|Rolling Downs Group|66623|3|Fully described|p108, pp238-245, pp256-267.|Late Cretaceous|Early Cretaceous|Widespread throughout Eromanga Basin. Thickness c.600 m. Generally poor outcrops. Has fair hydrocarbon reservoir (no source) potential, and good local seal potential. Porous sandstone units provide groundwater resources.|||Includes Wilgunya Subgroup (in Queensland), Wallumbilla Formation (at base), Allaru Mudstone and Winton Formation (at top).|Overlies Cadna-owie Formation. Is unconformably overlain by Eyre Formation. Unconformably overlies Yancannia Formation.|Alternation of sandstone-poor and sandstone-rich intervals deposited in a marine environment; ice-rafted dropstone boulders in lower units.|07-JUN-13
16267|Rolling Downs Group|66915|5|Briefly described|p4-5, p15-17|||In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||Wallumbilla Formation, Toolebuc Formation|||12-JAN-17
16267|Rolling Downs Group|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz and quartzite; conglomerate; quartzose sandstone; siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66921|6|Mentioned|Map legend|Cretaceous|Cretaceous||||Includes Cadna-owie Formation.|||
16267|Rolling Downs Group|67105|6|Mentioned|p661|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Cadna-owie Formation. Is overlain by Cordillo Silcrete.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Yancannia Formation. Unconformably overlies Warratta Group. Is overlain by Eyre Formation.|Marine white claystones, siltstones and fine-grained quartzose sandstones with bioturbation.|
16267|Rolling Downs Group|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Bunker Creek Formation and Warratta Group.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67402|4|Described|p179, p226-p230, p232, p309|Cenomanian|Aptian|Proven hydrocarbon seal in the Eromanga Basin with a combined thickness of up to 1500m; also present in the Laura Basin. Formerly the Battle Camp Shale and the Wolena Claystone.|||Includes the Allaru Mudstone, Toolebuc Formation and the Wallumbilla Formation|Overlies the Gilbert River Formation|Basal shale with minor silty and conglomeratic beds that is overlain by silty or sandy claystone with calcareous concretions.|
16267|Rolling Downs Group|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.|||Includes Wallumbilla Formation.|Underlain by Blythesdale Group.||
16267|Rolling Downs Group|68003|5|Briefly described|p52, p57 Fig.3-n, pp70-71, p127.|Early Cretaceous|Early Cretaceous|Surat Basin. Deposited in a major marine transgression-regression cycle.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|Overlies Bungil Formation and Drildool beds conformably.|Semiconsolidated clays and claystone with minor fine clayey quartz sandstone; coal and calcareous clay and calcarenite occur near the base; rare conglomerate and gravel.|
16267|Rolling Downs Group|68004|6|Mentioned|p131, p205.|Early Cretaceous|Early Cretaceous|Hosts the Lightning Ridge Opal Field. Mineral potential tracts and levels of certainty are discussed.||||||
16267|Rolling Downs Group|68069|5|Briefly described|Map legend, p2.|Cretaceous|Cretaceous|Surat Basin.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|||
16267|Rolling Downs Group|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Laura, Carpentaria and Eromanga Basins.|||Includes Wallumbilla, Griman Creek, Toolebuc, Normanton, Mackunda and Winton Formations, and Allaru Mudstone.|||
16267|Rolling Downs Group|68593|5|Briefly described|p3-4|Early Cretaceous|Early Cretaceous|See individual units.|||Purlawaugh, Griman Creek Formations; Surat Siltstone.|Overlies Bungil Formation.||
16267|Rolling Downs Group|68734|5|Briefly described|p218 Fig.2|Albian|Barremian|Eromanga Basin (SW and NE) and Surat Basin.|||Includes Winton, Mackunda, Oodnadatta, Toolebuc, Wallumbilla, and Griman Creek Formations; Coorikiana Sandstone; Bulldog Shale; Allaru Mudstone; and Surat Siltstone.|||16-JAN-17
16267|Rolling Downs Group|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Includes both marine and fluvial sedimentary rocks. Thick fluvial to coastal plain sequence.|||Includes Winton Formation, Mackunda Formation, Griman Creek Formation, Allaru Formation, Toolebuc Formation, Surat Siltstone, and Bulldog Shale.||Comprises carbonaceous and pyritic shale, siltstone, and coarse volcaniclastic sandstone with minor coal layers.|
16267|Rolling Downs Group|68901|6|Mentioned|p7 Fig. ii|||Eromanga Basin.|||Includes the Winton and Wallumbilla Formations.|||27-SEP-18
16267|Rolling Downs Group|69001|6|Mentioned|p2 Fig.1B, p30|Cretaceous|Cretaceous||||Includes the Doncaster Member.|||
16267|Rolling Downs Group|69297|6|Mentioned|p274 fig 4.3|Cenomanian|Early Cretaceous||||Includes the Wallumbilla Formation, Allaru Mudstone, Toolebuc Formation and the Normanton Formation.|||
16267|Rolling Downs Group|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|Central Carpentaria Basin.||||||12-JUL-16
16267|Rolling Downs Group|69457|5|Briefly described|p41:2, 6, 8, 12|||Whitehouse (1955). Applies to the succession in SW Eromanga Basin, from the top of the (ungrouped) Cadna-owie Formation to the top of the Winton Formation. Up to c.1700m thick.|||Wilgunya, Manuka, Marree Subgroups.|Overlies Cadna-owie Formation.||12-JUL-16
16267|Rolling Downs Group|69555|6|Mentioned|p46||||||Includes Winton Formation|||
16267|Rolling Downs Group|69591|6|Mentioned|p29|Cretaceous|Jurassic|||||||
16267|Rolling Downs Group|69594|4|Described|p521-522, p540, p573-574|Late Cretaceous|Aptian|Carpentaria, Laura Basins. Source of lateritic bauxite (at Weipa) and kaolin, formed by deep weathering during the Late Cretaceous regression. The Group acts as the confining beds for the main aquifers in the Basin. Not subdivided in the Laura Basin, where it is up to 212m thick and is equivalent to the Wallumbilla Formation in the Eromanga Basin. Coeval with Allaru Mudstone. Youngest deposit in the Laura Basin.|||Wallumbilla, Toolebuc Formations; Allaru Mudstone; Normanton Formation.|Conformably overlies Gilbert River Formation. Is equivalent to upper Battle Camp Formation, Wolena Claystone.|Undivided: basal marine unit of calcareous and glauconitic shales with minor siltstone and conglomerate, overlain by silty and sandy marine claystones with carbonate concretions.|
16267|Rolling Downs Group|69599|5|Briefly described|p601-602|Cretaceous|Cretaceous|Lateritisation of this unit produced the world's largest bauxite deposit at Weipa.|||Normanton Formation.|||
16267|Rolling Downs Group|69673|6|Mentioned|p156||||||Includes Wilgunya Subgroup, Manuka Subgroup|||
16267|Rolling Downs Group|69682|5|Briefly described|p93 Fig.1|Cretaceous|Cretaceous|Eromanga and Surat Basins.||||||
16267|Rolling Downs Group|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Winton and Wallumbilla Formations.|||
16267|Rolling Downs Group|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone?||Rounded, waterworn white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; sparse marine fossils; large quartzite dropstones. Bioturbated marine white claystones, siltstones and fine-grained quartzose sandstones.|16-SEP-15
16267|Rolling Downs Group|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. Included in a mapped unit of a marine sequence of semi-consolidated clay and claystone, minor fine quartz sandstone, coal and calcareous clay.||||||
16267|Rolling Downs Group|70207|6|Mentioned|p74|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Wilgunya Subgroup.|||
16267|Rolling Downs Group|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Wallumbilla, Toolebuc Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous||||Includes Wilgunya Subgroup.|||
16267|Rolling Downs Group|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous|2 un-named units: Marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation. Silicified variant.|||Includes 2 un-named units.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes Winton Formation, Allaru Mudstone, Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70651|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes unnamed sub-unit of marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation.|||Includes unnamed unit.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward fining sequence with sparse marine fossils and large rounded quartzite dropstones.|
16267|Rolling Downs Group|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Rounded quartz-rich gravel sourced from Namur Sandstone. Residual lag regolith and unconsolidated sediments also described.|||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70821|5|Briefly described|p21, p30-31, p33, p80, p109, p113-114|Late Cretaceous|Early Cretaceous|Eromanga, Surat Basins; Coonamble Embayment. Formerly included Hooray Sandstone. Sediments locally occupy palaeovalleys (eg Gongolgon).|||Wallumbilla, Toolebuc, Mackunda, Griman Creek, Winton Formations; Surat Siltstone; Allaru Mudstone.|Overlies Bungil or Cadna-owie Formations and Drildool beds. Is overlain unconformably by Glendower Formation.||
16267|Rolling Downs Group|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin.|||Griman Creek Formation.|||
16267|Rolling Downs Group|70860|6|Mentioned|p280-281|Cretaceous|Cretaceous|The main confining layer in the Great Artesian Basin.|||||A thick argillaceous marine sequence; mostly shallow-marine mudstone and siltstone.|
16267|Rolling Downs Group|71262|6|Mentioned|p9 Fig 7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71342|6|Mentioned|Ch6 p12|||Originally subdivided by Whitehouse in 1926 who also subdivided this groups constituents into three sets of bed based on ammonite fauna. This scheme however was called into question by Casey (1960) and Day (1969). The validity of the Roma and Tambo Series was demonstrated by later workers (Dickins, 1960; Ludbrook, 1966; Day; 1969 and Morgan, 1980).|||Includes the Morven Bed, Roma Series, Maryborough Beds and the Tambo Series.|||
16267|Rolling Downs Group|71409|5|Briefly described|p1058-1059, p1061|Cretaceous|Cretaceous|Carpentaria Basin. Likely proximal source rocks for heavy minerals in central Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.||||Is overlain locally by Bulimba Formation.|Siltstones and claystones; deeply weathered and bauxitised.|23-APR-18
16267|Rolling Downs Group|71415|5|Briefly described|p11-p12|Late Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Represents sedimentation from Early to Late Cretaceous before marine regression and closure of the Eromanga Basin (Exon and Senior 1976; Greenfield, Gilmore and Mills 2010).||||Uppermost unit of the Eromanga Basin. Underlain by Cadna-owie Formation.|Alternating sandstone, mudstone and calcareous units.|19-AUG-19
16267|Rolling Downs Group|71601|6|Mentioned|p121|||Geological province: Surat Basin.|||Includes Griman Creek Formation.|||
16267|Rolling Downs Group|71792|4|Described|p57-p58|Late Cretaceous|Early Cretaceous|Carpentaria Basin.|||||Grey mudstone, siltstone and fine sandstone, minor glauconitic sandstone.|
16267|Rolling Downs Group|71849|6|Mentioned|p8, p195|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71853|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|The two facies are mapped separately.|||||Siltstone and mudstone; minor glauconitic sandstone. Deeply weathered siltstone and mudstone; minor glauconitic sandstone.|
16267|Rolling Downs Group|71854|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous||||||Siltstone and mudstone with minor glauconitic sandstone; Deeply weathered siltstone and mudstone with minor glauconitic sandstone.|08-MAY-19
16267|Rolling Downs Group|71855|6|Mentioned|p20, p30|||Structure is briefly discussed.|||Includes the Toolebuc Formation.|||
16267|Rolling Downs Group|71863|5|Briefly described|p4|Late Cretaceous|Middle Jurassic|Carpentaria Basin. Deposited during a marine incursion.|||Includes the Wallumbilla Formation, the Toolebuc Formation, Allaru Mudstone and Normanton Formation.|||01-MAY-19
16267|Rolling Downs Group|71864|6|Mentioned|p13|||First described by Isbell (1957).|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|71890|6|Mentioned|p7|||Surat Basin.|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).|||Wallumbilla, Toolebuc, Mackunda, Winton, Normanton, Griman Creek FZs; Surat Siltstone; Allaru Mudstone.|Overlies Cadna-owie, Gilbert River, or Bungil FZ.||
16267|Rolling Downs Group|72914|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|72915|6|Mentioned|p12, p26|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group (map symbol suggests Cretaceous age), and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Represented in the Congararra 1 borehole by 41.15 m TVD thickness of interbedded claystone, siltstone, sandstone and arkose where the top portion is an indurated silcrete (to 23.53 m TVD), and is weathered to ~42 m TVD, before becoming fresh gravelly sand.|||||Interbedded claystone, siltstone, sandstone and arkose|
16267|Rolling Downs Group|72967|6|Mentioned|p5|||Carpenteria Basin.|||Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation, Gilbert River Formation|||
16267|Rolling Downs Group|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|73083|6|Mentioned|p51, p60-61, p68-69, p73|Mesozoic|Mesozoic|[Misspelt as Rolling Downs group on p61].|||Normanton Formation|||
16267|Rolling Downs Group|73144|6|Mentioned|p8|Cretaceous|Cretaceous|Carpentaria Basin. Contains units that constitute aquifers, partial aquifers, leaky aquitards and aquitards as well as host potential shale gas/oil plays and tight gas/oil.|||Normanton Formation, Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|Underlain by Gilbert River Formation.||17-OCT-22
16267|Rolling Downs Group|73147|5|Briefly described|p128-129|Albian|Aptian|Marine.|||Wallumbilla, Toolebuc, Normanton Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|73177|5|Briefly described|p1112|Late Jurassic|Late Jurassic|Relatively undeformed; gives a minimum age for the Alice Springs Orogeny.||||Unconformably overlies Ravendale Formation.||
16287|Roma Granite|24069|5|Briefly described|p282|Early Carboniferous|Early Carboniferous|Geological Province: Surat Basin.||||||
16287|Roma Granite|29413|6|Mentioned|p295|||||||||
16287|Roma Granite|29721|6|Mentioned|Table 269|||||||||
16287|Roma Granite|32578|6|Mentioned|Table 1|||L.Carb.||||||
16287|Roma Granite|33059|4|Described|Table 1|||L.Carb. See also P311||||||
16287|Roma Granite|33530|6|Mentioned|Table 1|||Lower Carb.||||||
16287|Roma Granite|36739|6|Mentioned|p22|||||||||
16287|Roma Granite|41159|6|Mentioned|p338|||||||||
16287|Roma Granite|41725|6|Mentioned|Fig.2|||||||||
16287|Roma Granite|42041|6|Mentioned|p222|||||||||
16287|Roma Granite|43008|5|Briefly described|map legend|||||||||
16287|Roma Granite|44208|14|Not recorded|p93|||||||||
16287|Roma Granite|44787|14|Not recorded|p123, Table||Early Carboniferous|||||||
16294|Roma granites|39273|6|Mentioned|Fig. 7|||||||||
16294|Roma granites|45110|4|Described|p66|||See also p25.||||||23-APR-18
16294|Roma granites|64855|4|Described|p16 Fig.2, p20 Tb.1, p22-25, p36|Early Carboniferous|Late Devonian|I-type and S-type granites, forming part of the basement to the Bowen Basin. Literature compilation gives minimum age of 355-360 Ma for the S-type granites. No reliable age data for the I-type granites. Some granites intrude the Timbury Hills Formation.||||||22-FEB-10
16294|Roma granites|64856|6|Mentioned|p43|||In base of wells in Roma area.|| ||||31-JAN-13
16294|Roma granites|67669|5|Briefly described|p11-12,17-18,22-23|Late Carboniferous|Late Carboniferous|Of Bowen Basin. Part of the basement assemblage to the Bowen Basin (Line 260), and crops on on the western margin boundary on Line 270. Intersected in Avondale South-1 borehole at 1.4 km depth, and represents basement as modelled on Line 270.||||Intrudes into Timbury Hills Formation.||
16294|Roma granites|68679|5|Briefly described|p371-372|Mississippian|Late Devonian|Houston (1964). Widespread on the Roma Shelf. Comprise two groups: S-type and I-type.|~360-355 Ma.|||Intrudes the Timbury Hills Formation.|More extensive S-type granites are mainly muscovite-biotite granite with lesser muscovite granite; less common I-type granites.|
16294|Roma granites|68731|5|Briefly described|p164, p166, p213 Fig 3.118|Early Carboniferous|Late Devonian|Probable S-type as indicated by the presence in some samples of altered cordierite. Appears as Roma Granites on p166.||||Non-conformably overlain by the Combarngo Volcanics.|Mainly biotite-muscovite bearing.|17-JUL-14
16294|Roma granites|69582|6|Mentioned|p94|Devonian|Devonian|||||||
16294|Roma granites|70033|6|Mentioned|p4, p40|||The latest Devonian - earliest Carboniferous Roma granites (Fergusson and Henderson 2013) provide a minimum age for the Timbury Hills formation.||||||
16294|Roma granites|71966|6|Mentioned|p989,991|Early Devonian|Early Devonian|Of Roma Shelf. Voluminous S-type granite magmatism immediately south of the Thomson Orogen in the late Devonian c. 380-360 Ma.||||||
16301|Ronlow beds|23430|4|Described|p523-524 Table 14.7|||Eromanga Basin Province. Maximum thickness <150 m.||||||
16301|Ronlow beds|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
16301|Ronlow beds|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16301|Ronlow beds|38199|6|Mentioned|p421|||||||||
16301|Ronlow beds|39943|6|Mentioned|Table 8A|||||||||
16301|Ronlow beds|41681|6|Mentioned|Table 5|||||||||
16301|Ronlow beds|42397|6|Mentioned|Fig.2 P3|||||||||
16301|Ronlow beds|42474|5|Briefly described|p26|||||||||
16301|Ronlow beds|42749|5|Briefly described|p31|||see also Fig.2 P27||||||
16301|Ronlow beds|43105|5|Briefly described|Fig.9,p15|||||||||
16301|Ronlow beds|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Warang Sandstone. Is overlain by Wallumbilla Formation.||
16301|Ronlow beds|66915|5|Briefly described|p9, p11 Fig.7|||Shown as Ronlow Beds in Fig.7.||||||12-JAN-17
16301|Ronlow beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Eromanga Basin.||||||
16301|Ronlow beds|69594|5|Briefly described|p526-527|Barremian|Bathonian|Vine et al. (1965). NE Eromanga Basin. Crops out in a discontinuous belt from near Torrens Creek to the Alice River near Barcaldine. 30-150m thick. Equivalent to the Hutton Sandstone-Hooray Sandstone interval. Deposition in fluvial channels and on a flood plain with minor swamps.||||Overlies Hutton Sandstone. Is overlain ?disconformably by the Doncaster Member (Wallumbilla Formation). Laterally continuous with Blantyre Sandstone.|Dominated by quartzose to sublabile sandstone, with lesser siltstone, mudstone and minor coal.|
16301|Ronlow beds|71710|6|Mentioned|p383 Fig 19|||Eromanga Basin.||||Underlain by Moolayember Formation.||
16301|Ronlow beds|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.||||Unconformably overlies Warang Sandstone. Is overlain by Doncaster Member (Wallumbilla FZ).||
16306|Rookwood Volcanics|22620|6|Mentioned|p187,9||Early Permian|||||||
16306|Rookwood Volcanics|23037|4|Described|p12,37,48,55-62,122||Early Permian|Max. thickness 300 m.||||||
16306|Rookwood Volcanics|23042|6|Mentioned|p9 Fig 2||Permian|||||||
16306|Rookwood Volcanics|23468|5|Briefly described|p 314|||||||||
16306|Rookwood Volcanics|24076|5|Briefly described|p397 Fig. 2|Late Permian|Early Permian|Max. thickness: 915m.  Geological Province: Yarrol Basin.||||||
16306|Rookwood Volcanics|24334|5|Briefly described|p48 Tb.1|Late Permian|Early Permian|Age: 250 - 290 Ma||||||
16306|Rookwood Volcanics|24399|5|Briefly described|p274, p277|Early Permian|Early Permian|See also p285.  Geological Province: New England Fold Belt.||||||
16306|Rookwood Volcanics|24491|3|Fully described|p20|Early Permian|Early Permian|Geological Province: Bowen Basin.||||||
16306|Rookwood Volcanics|24615|5|Briefly described|CD|Early Permian|Early Permian|[Pvr/f].  Rhyolitic lava and volcaniclastics including pumiceous breccia.||||||
16306|Rookwood Volcanics|30451|4|Described|p48|||||||||
16306|Rookwood Volcanics|30914|6|Mentioned|Map legend|Permian|Permian|||||||
16306|Rookwood Volcanics|31656|6|Mentioned|p9|||L.Perm. See also Fig. 3||||||
16306|Rookwood Volcanics|31657|4|Described|p95|||See also p102. Overlies & overlaps Youlambie Congl.||||||03-SEP-18
16306|Rookwood Volcanics|31658|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16306|Rookwood Volcanics|31659|4|Described|p63-64|Early Permian|Early Permian|Max. thickness: 3000ft. Spilitic pillow lava, basaltic flows, tuff, vitric tuff, mudstone. See also Table 1.||||||08-OCT-08
16306|Rookwood Volcanics|32496|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16306|Rookwood Volcanics|32577|5|Briefly described|p23|||||||||
16306|Rookwood Volcanics|34132|6|Mentioned|p2|||Lower Permian||||||
16306|Rookwood Volcanics|34138|6|Mentioned|Cor.Chart|||Kungurian - Kazanian||||||
16306|Rookwood Volcanics|34408|6|Mentioned|p185|||On Table||||||
16306|Rookwood Volcanics|36045|6|Mentioned|p332|||||||||
16306|Rookwood Volcanics|37749|6|Mentioned|p194|||||||||
16306|Rookwood Volcanics|37860|5|Briefly described|p572|||||||||
16306|Rookwood Volcanics|38081|5|Briefly described|Table 1|||||||||
16306|Rookwood Volcanics|38153|6|Mentioned|p373|||||||||
16306|Rookwood Volcanics|38406|6|Mentioned|p11|||||||||
16306|Rookwood Volcanics|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16306|Rookwood Volcanics|39252|6|Mentioned|Fig.13|||||||||
16306|Rookwood Volcanics|39445|5|Briefly described|Table 8|||||||||
16306|Rookwood Volcanics|40960|6|Mentioned|p231|||||||||
16306|Rookwood Volcanics|41246|6|Mentioned|Map legend|Permian||||||||
16306|Rookwood Volcanics|41474|6|Mentioned|p62|||||||||
16306|Rookwood Volcanics|41475|6|Mentioned|p70|||||||||
16306|Rookwood Volcanics|41922|4|Described|Table 1P9|||||||||
16306|Rookwood Volcanics|41924|5|Briefly described|p29|||See also P31||||||
16306|Rookwood Volcanics|43017|6|Mentioned|p377|||||||||
16306|Rookwood Volcanics|43994|14|Not recorded|Map Legend||Permian|||||||
16306|Rookwood Volcanics|43998|4|Described|p12,14,map||Early Permian|||||||
16306|Rookwood Volcanics|44002|14|Not recorded|Map Legend|||||||||
16306|Rookwood Volcanics|44003|14|Not recorded|Map Legend||Permian|||||||
16306|Rookwood Volcanics|44337|5|Briefly described|Map Legend||Early Permian|Lithology.||||||
16306|Rookwood Volcanics|44424|14|Not recorded|p293-301|||||||||
16306|Rookwood Volcanics|45071|3|Fully described|Table 1|||||||||
16306|Rookwood Volcanics|48898|2|Defined|p24|Permian|Permian|See also PP1,2,7,12 etc||||||
16306|Rookwood Volcanics|48915|6|Mentioned|Table 1|||Permian. See also PP4,10||||||
16306|Rookwood Volcanics|50209|5|Briefly described|Map Legend|Permian|Permian|||||||
16306|Rookwood Volcanics|50213|5|Briefly described|Map legend|Permian|Permian|Overlie Youlambie Conglomerate.||||||17-MAY-04
16306|Rookwood Volcanics|50215|5|Briefly described|Map Legend|Early Permian|Early Permian|Basaltic pillow lava and breccia. minor chert, sandstone and siltstone; some dolerite sills and dykes.||||||18-JUN-09
16306|Rookwood Volcanics|50317|5|Briefly described|Map Legend|Permian|Permian|||||||
16306|Rookwood Volcanics|50602|5|Briefly described|Map Legend|Late Permian|Early Permian|Basaltic pillow lava and breccia, minor chert, sandstone, siltstone. Overlies: Youlambie Conglomerate.  Underlies: Back Creek Group.||||||30-JUN-04
16306|Rookwood Volcanics|60282|5|Briefly described|p1, p10|Early Permian|Early Permian|Mainly basalt and high-level mafic intrusives, with minor rhyodacite lava, volcanilithic breccia and sandstone and mudstone. Overlies the Youlambie Conglomerate in the north.  Geological Province: Yarrol Province.||||||28-APR-05
16306|Rookwood Volcanics|60481|5|Briefly described|Map Legend|Early Permian|Early Permian|Basaltic pillow lava and breccia, minor chert, sandstone, siltstone; some dolerite sills or dykes.||||||
16306|Rookwood Volcanics|60557|5|Briefly described|p19 Fig. 5b, p25|Early Permian|Early Permian|Overlie the Youlambie Conglomerate; have overthrust the Back Creek Group.  See also p20 Fig. 5c.||||||09-JUN-05
16306|Rookwood Volcanics|61035|5|Briefly described|p12, p39, p40, p41, p42|Early Permian|Early Permian|Tectonic relaitionship to the Glenprairie and Wongrabry beds. Age based on fossil evidence. Geological Province: Yarrol Province. Consists of altered aphyric basalt and minor chert, locally intruded by small gabbro or dolerite bodies.||||||07-FEB-11
16306|Rookwood Volcanics|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|||||||
16306|Rookwood Volcanics|61777|5|Briefly described|p224|Artinskian|Early Permian|Geological Province: Yarrol Province. Mafic pillow lavas, high-level mafic intrusives and minor sedimentary rocks.||||||07-FEB-11
16306|Rookwood Volcanics|61778|5|Briefly described|p243||Early Permian|Dominated by mafic volcanics.||||||07-FEB-11
16306|Rookwood Volcanics|61906|5|Briefly described|p141, p142|Early Permian|Early Permian|Comprises spilitic pillow lava, agglomerate, volcanic breccia, chert, vitric tuff and tuffaceous sandstone/siltstone. Geological Province: along edge of the Bowen Basin.||||||
16306|Rookwood Volcanics|65114|5|Briefly described|p383 Tb.1, p397|Early Permian||Tectonic unit: Northern New England Orogen, Gogango Thrust Belt; considered part of the extensional phase; located well to the east of the present-day Bowen Basin||||||
16306|Rookwood Volcanics|65388|3|Fully described|p51-55, p48, 31, 35, 42, 46, 50, 58|Artinskian|Artinskian|Grantleigh Subprovince, Yarrol Province. Conformably overlie and apparently interfinger with Youlambie Conglomerate, although this may be a thrust contact. Apparently conformably (p46) or unconformably (p58) overlain by Moah Creek beds. Intruded by unnamed Triassic granite. Defined by Malone and others (1969); type area in Melaleuca Creek. Artinskian foraminiferids found in upper part of unit. May correlate with Nogo Subprovince units. In type section: Mainly of lavas, with minor volcanic breccia; chert, volcaniclastic sandstone and siltstone. See also p70, 81, 123, 156, 174, 175, 176, 338, 395, 435, 439, 445, 446, 447.||||||
16306|Rookwood Volcanics|68008|3|Fully described|p2, p131-132, p134, p137-139, p147-157|Permian|Permian|See also p179, p248, p292, p322-323, p437, p480-481, p485, p491, p569. Malone et al. (1969) in the Duaringa 250k sheet area; subsequently extended by Kirkegaard et al. (1970) and Dear et al. (1971). Areas of outcrop listed and mapped. Named after Rookwood homestead. No type section; the type area is along Melaleuca Creek. Lithologies described and illustrated in detail. Thickness is probably much less than the estimated 3-4.5 km of Clare (1993). Part of an extension-related package: typical oceanic back-arc chemistry. Geochemistry detailed; may be comagmatic with Kyle Mohr Igneous Complex. Early to Middle Permian age from fossils and stratigraphic relationships; roughly coeval with Berserker Group. Hosts VHMS deposit at Develin Creek. Is intruded by Bucknalla Gabbro.||||Conformably overlies and interfingers with Youlambie Conglomerate; elsewhere is thrust over or under that unit. Underlies Dinner Creek Conglomerate, and Back Creek Group (and faulted against it).|Extensive pillow basalts and high-level mafic intrusives with minor dacitic to rhyolitic lava, volcaniclastic breccia and sandstone, siltstone and mudstone.|
16306|Rookwood Volcanics|68359|6|Mentioned|p9|||||||||
16306|Rookwood Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Yarrol Province.||||||
16306|Rookwood Volcanics|68679|5|Briefly described|p308, p312-313, p337-338, p342-347, p352|Artinskian|Artinskian|See also p380, p385, p426, p469-470. Described by Malone et al. (1969) and numerous others (listed). Grantleigh Subprovince, Northern Yarrol Province. Backarc submarine volcanic rocks in an extensional regime; similar to oceanic basalts. Probably comagmatic with Kyle Mohr Igneous Complex. Hosts the Cu-(Zn) VAMS deposit at Develin Creek.||||Conformably overlies Youlambie Conglomerate. Is overlain unconformably by Moah Creek beds. Is thrust over Back Creek Group. Is intruded by Bucknalla Gabbro.|Mainly aphyric to porphyritic basalt, usually extensively altered, with local ovoid pillows and hyaloclastic breccia, and high-level mafic intrusives; minor dacitic to rhyolitic lava, volcaniclastic breccia, sandstone, siltstone and mudstone.|
16306|Rookwood Volcanics|68822|6|Mentioned|p338|Artinskian|Artinskian|Bimodal. MORB-type geochemistry.||||||
16306|Rookwood Volcanics|71115|6|Mentioned|p193|||||||||
16306|Rookwood Volcanics|71702|6|Mentioned|179|||Backarc-rift related rocks.||||||
16306|Rookwood Volcanics|73197|5|Briefly described|p474, p475 Fig.6, p477-478|Lopingian|Guadalupian|New England Orogen, northern. Coeval with Owl Gully Volcanics, Berserker Group, Double Mountain Volcanics, Peninsula Range Volcanics and Kyle Mohr Igneous Complex. Typical oceanic back-arc geochemical signature.|||||Bimodal basaltic-rhyolitic lavas and pyroclastics.|
16306|Rookwood Volcanics|73450|6|Mentioned|p53|||||||||
16308|Rooney Point beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
16308|Rooney Point beach sand|39495|6|Mentioned|p142|||||||||
16308|Rooney Point beach sand|62102|5|Briefly described|p367 Tb. 1|||Informal name for morphostratigraphic unit on southeast Queensland coast.||||||
16348|Roseneath Shale|13497|3|Fully described|iv, p69 fig 6.1, p70|Kungurian|Kungurian|Cooper Basin. Defined by Gatehouse (1972). Name derived from Roseneath Parish in Carruthers County, South West Queensland. Originally included as one of three units in the Moomba Formation before being raised to formation status by Gatehouse (1972). A type section is briefly mentioned. Maximum thickness of 100m. Petrography briefly discussed. A cross section where it contacts the Daralingie Formation is given on p99. This unit forms an important regional seal over the Epsilon Formation. Wireline log results are discussed. See also p93-p97, p99, p117, p129, p131, p160, p170-p175.||Gidgealpa Group||Intertongues with and conformably overlies the Epsilon Formation. Conformably overlain by the Daralingie Formation. Unconformably overlain by the Toolachee Foramtion.|Light to dark brown-grey or olive-grey siltstone, mudstone and minor sandstone. Siltstones are micromicaceous with minor fine-grained pyrite. Sandstone interbeds are pale brown and fine-grained.|
16348|Roseneath Shale|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
16348|Roseneath Shale|22839|6|Mentioned|P33|||||||||
16348|Roseneath Shale|22883|6|Mentioned|P29|||||||||
16348|Roseneath Shale|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Of the Gidgealpa Group.||||||17-JAN-08
16348|Roseneath Shale|23155|4|Described|p21|Early Permian|Early Permian|The Roseneath Shale is diachronous, younging southwest. The unit is up to 90m thick in the Mettika Embayment. Of Gidgealpa Group, Cooper Basin.||||||17-SEP-08
16348|Roseneath Shale|23340|6|Mentioned|12|||||||||
16348|Roseneath Shale|23375|4|Described|Fig2 p265,267,274,285||Kungurian|In the Cooper Basin.||||||17-JAN-08
16348|Roseneath Shale|23832|4|Described|p330|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
16348|Roseneath Shale|24210|5|Briefly described|p133 Fig. 2|Permian|Permian|Of the Gidgealpa Group.  Overlies the Epsilon Formation and Murteree Shale.  Geological Province: Cooper Basin.||||||
16348|Roseneath Shale|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
16348|Roseneath Shale|29391|6|Mentioned|Table 5|||Appears on P23.||||||
16348|Roseneath Shale|29721|6|Mentioned|p161|||||||||
16348|Roseneath Shale|30540|6|Mentioned|Fig.6|||||||||
16348|Roseneath Shale|30544|6|Mentioned|p53|||Map legend||||||
16348|Roseneath Shale|30825|6|Mentioned|p37|||||||||
16348|Roseneath Shale|30873|2|Defined|p13|Permian|Permian|Part of Gidgealpa Group.||||||14-APR-08
16348|Roseneath Shale|30921|6|Mentioned|Map legend|Artinskian|Sakmarian|Sakmarian - Artinskian||||||
16348|Roseneath Shale|33074|6|Mentioned|p260|||||||||
16348|Roseneath Shale|33331|6|Mentioned|p39|||||||||
16348|Roseneath Shale|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
16348|Roseneath Shale|33976|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|34839|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|35067|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|35068|6|Mentioned|Fig.3|||Discussed P60.||||||
16348|Roseneath Shale|35279|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
16348|Roseneath Shale|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
16348|Roseneath Shale|35845|6|Mentioned|p24|||See also P73.||||||
16348|Roseneath Shale|36099|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|36910|6|Mentioned|p62|||||||||
16348|Roseneath Shale|36917|6|Mentioned|Fig.1|||||||||
16348|Roseneath Shale|37855|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|37917|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|38977|6|Mentioned|p1422|||||||||
16348|Roseneath Shale|39252|5|Briefly described|p20|||||||||
16348|Roseneath Shale|39254|5|Briefly described|p46|||||||||
16348|Roseneath Shale|39261|6|Mentioned|Fig. 9|||||||||
16348|Roseneath Shale|39264|6|Mentioned|Fig. 13|||||||||
16348|Roseneath Shale|39276|6|Mentioned|Fig. 2|||||||||
16348|Roseneath Shale|39445|5|Briefly described|Table 8|||||||||
16348|Roseneath Shale|39478|6|Mentioned|Table 1|||||||||
16348|Roseneath Shale|39494|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|40030|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|40056|6|Mentioned|p11|||||||||
16348|Roseneath Shale|40249|6|Mentioned|p45|||||||||
16348|Roseneath Shale|40544|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|41099|6|Mentioned|p190|||||||||
16348|Roseneath Shale|41131|5|Briefly described|Table 1|||||||||
16348|Roseneath Shale|41164|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|41183|6|Mentioned|Fig.3 p308|||||||||
16348|Roseneath Shale|41189|6|Mentioned|Fig.4|||||||||
16348|Roseneath Shale|41198|6|Mentioned|Table 1|||||||||
16348|Roseneath Shale|41214|6|Mentioned|Fig.3|||||||||
16348|Roseneath Shale|41247|6|Mentioned|Fig.5|||||||||
16348|Roseneath Shale|41267|6|Mentioned|Fig.2|||||||||
16348|Roseneath Shale|41288|6|Mentioned|p159|||||||||
16348|Roseneath Shale|41595|6|Mentioned|p42|||||||||
16348|Roseneath Shale|41707|6|Mentioned|Fig.8|||||||||
16348|Roseneath Shale|41720|6|Mentioned|p373|||||||||
16348|Roseneath Shale|42085|6|Mentioned|Fig.2 P374|||||||||
16348|Roseneath Shale|42746|5|Briefly described|p6|||||||||
16348|Roseneath Shale|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
16348|Roseneath Shale|43002|5|Briefly described|Fig.2,p135|||||||||
16348|Roseneath Shale|43018|5|Briefly described|Table 1,p386|||||||||
16348|Roseneath Shale|43105|5|Briefly described|Fig.7,p13|||||||||
16348|Roseneath Shale|43570|5|Briefly described|Fig.2,p535,544,545||Kungurian|||||||
16348|Roseneath Shale|44133|5|Briefly described|p65 Fig. 8.3, 85|Kungurian|Kungurian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Overlies: Epsilon Formation. Underlies: Daralingie Formation.||||||
16348|Roseneath Shale|46849|6|Mentioned|Fig. 7|||||||||
16348|Roseneath Shale|60386|6|Mentioned|p296|Kungurian|Kungurian|Cooper Basin. Non-marine.||||||
16348|Roseneath Shale|60717|5|Briefly described|p40 Fig. 2|Kungurian|Kungurian|Of Gidgealpa Group. Overlies Epsilon Formation; underlies Daralingie Formation. Geological province: Cooper Basin.||||||
16348|Roseneath Shale|61615|5|Briefly described|p302, p302 Fig. 2, p304|Early Permian|Early Permian|Of Gidgealpa Group. Underlain by Epsilon Formation. Geological Province: Cooper Basin.||||||30-APR-13
16348|Roseneath Shale|61616|6|Mentioned|p330 Fig. 2|Early Permian|Early Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
16348|Roseneath Shale|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
16348|Roseneath Shale|62537|6|Mentioned|p191 Fig.2. |Early Permian|Early Permian|Cooper Basin.||Unit in Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|63832|6|Mentioned|p131 fig 2|Kungurian|Kungurian|Cooper Basin.||||||
16348|Roseneath Shale|63978|2|Defined|p15, Fig. 3|Middle Permian|Early Permian|Conformable over/intertongues with Epsilon Fm; overlain/intertongues with Daralingie Fm; unconformable below Toolachee Fm.in places. Max. thick: 99m. Laminated siltstone, mudstone and lesser sandstone (carbonaceous). more lith.included. In Cooper Basin.||||||07-FEB-11
16348|Roseneath Shale|64048|5|Briefly described|p63, p64 Tb. 2|||Geological Province: Cooper Basin. Acts as the seal for Epsilon Formation reservoirs.||||||07-FEB-11
16348|Roseneath Shale|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Permian|Permian|Cooper Basin.||||Underlies Daralingie [Beds] Formation, overlies Epsilon and Patchawarra Formations.||11-DEC-15
16348|Roseneath Shale|64665|5|Briefly described|p53 Fig.2.|Middle Permian|Middle Permian|Cooper Basin.||||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|65489|5|Briefly described|p45, p48-49, p96, p131-132, p143|Kungurian|Kungurian|Cooper Basin. Relatively little hydrocarbon source potential. Regional seal of the Epsilon Formation.||Unit in Gidgealpa Group.||Overlies Epsilon Formation and Murteree Shale. Is overlain by Daralingie Formation.|Lacustrine shale unit.|
16348|Roseneath Shale|65925|5|Briefly described|Appendix 2.||||||||Siltstone, shaly, with minor sandstone lenses. Lacustrine, diachronous.|
16348|Roseneath Shale|67402|5|Briefly described|p90, p90 fig CPR4|||Cooper Basin. 50-100m thick. Distal lacustrine deposits. Forms regionally extensive seal to the Epsilon Formation. See also p91 tbl CPR1, p92, p93, p96, p98, p101 tbl CPR2.||Gidgealpa Group||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.|Laminated carbonaceous siltstone, mudstone and minor thin beds of fine-grained sandstone.|
16348|Roseneath Shale|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Guadalupian||Gatehouse (1972). Along with the Murteree Shale and Epsilon Formation, the Roseneath Shale replaces the Moomba Formation. ~ 20-100 m thick. Palynofloral assemblages suggest latest Kungurian(?)-early Wordian (Price 1997).||Of the Gidgealpa Group.||Conformably underlain by the Epsilon Formation. Conformably/unconformably overlain by the Daralingie and Toolachee Formations respectively. Intertongues with the Epsilon and Daralingie Formations.|Includes laminated, carbonaceous, micro-micaceous siltstones with pyrite and siderite, and mudstone and lesser fine sandstone, the latter forming beds rarely > 2 m thick.|18-JUL-14
16348|Roseneath Shale|69023|5|Briefly described|p81, p82 Fig.18, p85|Permian|Permian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||||
16348|Roseneath Shale|69454|5|Briefly described|p38:4|Wordian|Kungurian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
16348|Roseneath Shale|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Daralingie Formation, overlies Epsilon Formation||
16348|Roseneath Shale|69797|5|Briefly described|p17 Fig.2|Early Permian|Early Permian|Age: Kungarian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
16348|Roseneath Shale|69946|5|Briefly described|p9, p36, p45, p54|Kungurian|Kungurian|Cooper Basin. Lacustrine.||Unit in Gidgealpa Group.||Overlies Epsilon and Patchawarra Formations. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
16348|Roseneath Shale|70317|6|Mentioned|p33-34, 36|Early Permian|Early Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|70823|4|Described|iv, p1, p3, p6|Wordian|Roadian|Cooper Basin. Hosts shale gas plays. Seismic reflection, palynological and outcrop characteristics briefly discussed. On the basis of spore pollen zones this unit has been dated at 269.6 Ma and 266.8 Ma. Up to 240m thick. Deposited in a lacustrine environment. Contains potential source rock facies. See also p14-p15, p25-p27, p38, p40-p41, p54, p59, p64-p65, p78, p82-p83.||Gidgealpa Group||Intertongues with and conformably overlies the Epsilon Formation. Conformably overlain by the Daralingie Formation.|Light to dark brown-grey siltstone, mudstone and minor fine-grained sandstone units.|
16348|Roseneath Shale|70824|4|Described|p1, p3, p7-p9, p30-p31|Wordian|Roadian|Cooper Basin. Hosts shale gas plays. Deposited in a lacustrine environment. Up to 240m thick. Forms a hydrocarbon seal over the Epsilon Formation. Outcrop, areal extent and source rock geochemistry are discussed. See also p77-p83, p108-p109, p113, p123.||||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.|Light to dark brown-grey siltstone, mudstone and minor fine-grained sandstone units.|
16348|Roseneath Shale|70946|5|Briefly described|p1087, p1089-1091, p1096|Permian|Early Permian|Cooper Basin. Hosts shale gas plays. Up to 194m thick. HyLogging was combined with XRD and core petrology to target fracture stimulation. Deposited in lacustrine with interbedded fluvio-deltaic transgressive/regressive shoreface environments.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.|Siltstones, siliceous (and sideritic in part) mudstones.|08-OCT-18
16348|Roseneath Shale|71059|6|Mentioned|p6 Fig.5|||Cooper Basin.||||||
16348|Roseneath Shale|71265|5|Briefly described|p589|Wordian|Roadian|Cooper Basin.||Gidgealpa Group.||Overlies Epsilon Formation. Is overlain by Daralingie Formation.||
16348|Roseneath Shale|71342|5|Briefly described|Ch5 p3, Ch5 p9|Kazanian|Kungurian|Cooper Basin. Deposited in a lacustrine environment.  Palynological zone is given in fig 5.3 Ch5 p36. See also Ch5 p36, Ch5 p45, Ch5 p54, Ch7 p13.||Gidgealpa Group||||
16348|Roseneath Shale|71701|5|Briefly described|p155|Wordian|Roadian|Cooper Basin.||Gidgealpa Group||Overlies the Epsilon Formation. Overlain by the Daralingie Formation.||
16348|Roseneath Shale|71863|6|Mentioned|p2|Paleozoic|Paleozoic|Cooper Basin.||||||
16348|Roseneath Shale|72297|6|Mentioned|p742|||Cooper Basin. Acts as a regional seal.||||||
16348|Roseneath Shale|73167|6|Mentioned|p662, p664|late Permian|late Permian|Cooper Basin. Deposited in an east-to-west late Permian transgression of fluvio-deltaic, shoreface and lacustrine sediments.||||||
16348|Roseneath Shale|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine environment.||||||
16348|Roseneath Shale|73251|6|Mentioned|p62|Cisuralian|Cisuralian|Cooper Basin. Lacustrine depositional environment. Hydrocarbon source rock.||Gidgealpa Group||Underlain by Epsilon Formation. Overlain by Daralingie Formation.||
16348|Roseneath Shale|73343|6|Mentioned|p337-338|Late Permian|Late Permian|Cooper Basin.||||Underlain by Murteree Shale. Unconformably overlain by Toolachee Formation. Equivalent to Daralingie Formation.||
16348|Roseneath Shale|73479|5|Briefly described|p156 Fig.2, p159, p163|Permian|Permian|Cooper Basin. Fluvio-deltaic/lacustrine depositional environment. Highly efficient regional seal.|ca 260 Ma|||Unconformably underlies Toolachee Formation||
16348|Roseneath Shale|73495|6|Mentioned|p497, p499-500|Captainian|Wordian|Cooper Basin. Part of the REM succession.||||Underlain by Epsilon Formation. Overlain by Daralingie Formation.||
16354|Roses Pride Formation|42054|6|Mentioned|p272|||||||||
16369|Rossmoya beds|41576|4|Described|p22|||See also Table 1||||||
16369|Rossmoya beds|41577|6|Mentioned|Map legend|Tertiary||||||||
16369|Rossmoya beds|41922|4|Described|Table 1, p8|||||||||23-NOV-15
16369|Rossmoya beds|42054|6|Mentioned|p272|||||||||
16369|Rossmoya beds|50209|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
16369|Rossmoya beds|60557|5|Briefly described|p19 Fig. 5b, p28|Tertiary|Tertiary|||||||
16369|Rossmoya beds|68008|4|Described|p281-283, p297|Eocene|Eocene|Sedimentary fill of the Rossmoya Basin. Insufficient information for a formal definition. Lacustrine deposits. Possibly up to 400m thick. Early Tertiary age by similarity with other basins in the region. Hosts a bright red iron-rich zone of uncertain thickness.||||Overlies Alton Downs Basalt.|Pale grey to pale greenish-grey mudstone, sandy mudstone, medium- and fine-grained lithic quartz sandstone, and interbedded carbonaceous sequences of black lignitic oil shale and mudstone. No thick or high-grade oil shale is present.|
16369|Rossmoya beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
16369|Rossmoya beds|68679|6|Mentioned|p312-313|Paleogene|Paleogene|Northern New England Orogen.||||||
16369|Rossmoya beds|69599|5|Briefly described|p586, p589|Eocene|Eocene|Rossmoya Basin. Subsurface. Up to 190m thick. RELATED UNITS (continued): Also correlated (at least partly) with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Water Park Creek and Herbert Creek beds; Flinders Dolomite; see COMMENTS for more.|Siltstone, claystone, oil shale, carbonaceous shale and sandstone.|
16369|Rossmoya beds|69952|6|Mentioned|p75|Oligocene|Paleocene|||||||
16392|Routh Dacite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Kungaree Volcanic Subgroup. Thickness: Up to 1000m. Geological Province: Georgetown Region.||||||28-MAY-15
16392|Routh Dacite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V20. ?A-Type.||||||
16392|Routh Dacite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16392|Routh Dacite|43259|4|Described|Appendix 1,p2.||Carboniferous|of Kungaree Volcanic Subgroup.||||||
16392|Routh Dacite|43740|4|Described|p9|||||||||
16392|Routh Dacite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Kungaree Volcanic Subgroup (Newcastle Range Volcanic Group).||||||
16392|Routh Dacite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Kungaree Volcanic Subgroup.|||Grey to brown, porphyritic dacite and moderately crystal-rich to crystal-rich dacitic ignimbrite with variable amounts of chlorite; probably includes intrusive equivalents; lesser dacitic volcanic arenite to very coarse volcanic rudite.|
16392|Routh Dacite|68576|5|Briefly described|Q_11: p22-23|Carboniferous|Carboniferous|||Newcastle Range Volcanic Group.||||
16392|Routh Dacite|70207|5|Briefly described|p82, p85|Permian|Permian|Northern part of the Newcastle Range.||Kungaree Volcanic Subgroup.|||A-type.|
16404|Roxmere Quartzite|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Mount Albert Group. Sandstone, quartzite, siltstone. Underlies: Mount Birnie Beds. Overlies: Corella Formation||||||27-AUG-04
16404|Roxmere Quartzite|22460|6|Mentioned|Fig 1 p446.|||||||||
16404|Roxmere Quartzite|22461|5|Briefly described|p468|||Assigned to Mt Albert Group but may belong to the Mary Kathleen Group?||||||02-APR-07
16404|Roxmere Quartzite|22483|5|Briefly described|Fig 1 p415|||also see Figure 2 p416.||||||
16404|Roxmere Quartzite|22523|6|Mentioned|Fig1p364|||||||||
16404|Roxmere Quartzite|23070|5|Briefly described|p769 (fig 1)|||||||||
16404|Roxmere Quartzite|23333|5|Briefly described|1114 Fig.1|||||||||
16404|Roxmere Quartzite|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16404|Roxmere Quartzite|30531|6|Mentioned|p20|||||||||
16404|Roxmere Quartzite|30532|3|Fully described|p115|||||||||
16404|Roxmere Quartzite|31043|4|Described|p54|||See also Fig. 1||||||
16404|Roxmere Quartzite|32660|5|Briefly described|Table 5|||||||||
16404|Roxmere Quartzite|33900|6|Mentioned|p15|||See also p18.||||||02-APR-07
16404|Roxmere Quartzite|35295|6|Mentioned|p602|||||||||
16404|Roxmere Quartzite|37568|5|Briefly described|p84|||||||||
16404|Roxmere Quartzite|37862|6|Mentioned|p587|||||||||
16404|Roxmere Quartzite|38234|6|Mentioned|Fig.2|||||||||
16404|Roxmere Quartzite|38235|6|Mentioned|p116|||||||||
16404|Roxmere Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16404|Roxmere Quartzite|38833|6|Mentioned|p162|||||||||
16404|Roxmere Quartzite|38834|6|Mentioned|p163|||||||||
16404|Roxmere Quartzite|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16404|Roxmere Quartzite|39445|6|Mentioned|p43|||See also Table 2||||||
16404|Roxmere Quartzite|39496|4|Described|p13|||||||||
16404|Roxmere Quartzite|39622|6|Mentioned|Fig.2|||||||||
16404|Roxmere Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
16404|Roxmere Quartzite|40840|6|Mentioned|Map legend|||||||||
16404|Roxmere Quartzite|41464|6|Mentioned|Map legend|Proterozoic||||||||
16404|Roxmere Quartzite|41556|6|Mentioned|Map legend|Proterozoic||||||||
16404|Roxmere Quartzite|41568|4|Described|p12|||||||||
16404|Roxmere Quartzite|41791|6|Mentioned|p255|||||||||
16404|Roxmere Quartzite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Part of the Mary Kathleen Group.  Feldspathic sandstone.||||||09-FEB-09
16404|Roxmere Quartzite|44270|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
16404|Roxmere Quartzite|44271|14|Not recorded|p32|||Overlies Corella Formation. Probably contemporaneous with Knapdale Quartzite.||||||
16404|Roxmere Quartzite|44275|14|Not recorded|Map Legend|||||||||
16404|Roxmere Quartzite|44276|2|Defined|p12,18,Tb.1,map|||||||||
16404|Roxmere Quartzite|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
16404|Roxmere Quartzite|44278|2|Defined|p7,map,Tb.1||Paleoproterozoic|||||||07-NOV-08
16404|Roxmere Quartzite|44989|14|Not recorded|Not recorded|||||||||
16404|Roxmere Quartzite|45161|4|Described|p50|||||||||
16404|Roxmere Quartzite|45166|4|Described|p32|||||||||
16404|Roxmere Quartzite|45287|14|Not recorded|p.226,227|||||||||
16404|Roxmere Quartzite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
16404|Roxmere Quartzite|49009|6|Mentioned|p45|||||||||
16404|Roxmere Quartzite|50100|5|Briefly described|p11, p13 Fig. 4, p20|Statherian|Statherian|Feldspathic and quartz sandstone with minor calcareous and micaceous siltstone, calcareous sandstone, conglomerate and breccia.  Geological Province: Eastern Fold Belt Province.||||||02-APR-07
16404|Roxmere Quartzite|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
16404|Roxmere Quartzite|50332|4|Described|p16, p21|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group. Overlain by Marimo Slate. Age: 1695-1600Ma. Geological Province: Eastern Fold Belt Province. Consists of sandstone with minor siltstone, conglomerate and breccia.||||||07-FEB-11
16404|Roxmere Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite, minor siltstone.||||||
16404|Roxmere Quartzite|61922|5|Briefly described|p12 Fig. 5|||See also p16 Fig. 8.||||||
16404|Roxmere Quartzite|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Isa Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||
16404|Roxmere Quartzite|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
16404|Roxmere Quartzite|61936|5|Briefly described|p190 Fig. 3|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
16404|Roxmere Quartzite|62047|6|Mentioned|p90 Fig.1 |||||||||
16404|Roxmere Quartzite|63866|5|Briefly described|p62|Statherian|Statherian|Numeric age is interpreted as the maximum depositional age.|c. 1710 Ma (Neumann, unpub.)|||||
16404|Roxmere Quartzite|64248|6|Mentioned|p37|||(Foster and Austin, 2008) proposed including this unit in Young Australia Group.||||||
16404|Roxmere Quartzite|64250|6|Mentioned|p13 fig 5, p11 fig 3, p20|||Cloncurry Fold Belt, Mount Isa Inlier.||Of Young Australia Group.||Included in Young Australia Group that it tectonically overlies. Thrust over Corella Formation, Staveley Formation, Marimo Slate.|Fault-bounded blocks of feldspathic and quartz sandstone.|15-MAR-18
16404|Roxmere Quartzite|65396|5|Briefly described|p16-17, p169, p183-184, p189-190, p218|||Eastern Fold Belt, Leichhardt Superbasin. Cover Sequence 3. Detailed discussion on its assignation to basal Young Australia Group: conflicting stratigraphic positions. Its basal contacts are commonly faults or breccia zones.||Young Australia Group||Tectonically overlies Young Australia Group. Overlain by Answer Slate.|Feldspathic, quartz sandstones, quartzite.|
16404|Roxmere Quartzite|66913|5|Briefly described|p170 fig 1||||1690-1650 Ma|||||
16404|Roxmere Quartzite|67323|5|Briefly described|p18-20, p24, p33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot. Marimo-Staveley and Doherty-Fig Tree Gully Domains, Mount Isa Inlier, Calvert Superbasin. Forms synforms and antiforms interpreted as limbs of nappe structures.|~1710 Ma (max. depositional age).|||Gradationally overlies Staveley Formation. Is intruded by Williams Supersuite.|Thick-bedded, quartzose to feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination.|
16404|Roxmere Quartzite|68021|6|Mentioned|p135 fig 4|Statherian|Statherian|Eastern Succession.||||Partly equivalent to Surprise Creek Formation?||
16404|Roxmere Quartzite|68146|5|Briefly described|p3, p6, p90-98, p199-200, p211|||Doherty-Fig Tree Domain. Forms the prominent southern end of Fig Tree Range. Whole-rock Sm-Nd isotopic data tabulated.|1711 +/- 4 Ma maximum depositional age.|||Overlies Staveley Formation. Correlated with Knapdale and Deighton Quartzites.|Purplish grey, thin- to very thick-bedded, very fine- to fine-grained quartzose sandstone.|
16404|Roxmere Quartzite|68542|6|Mentioned|p16 fig 4|||||||||
16404|Roxmere Quartzite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Staveley Formation under the symbol, -Ps.||||||
16404|Roxmere Quartzite|68576|6|Mentioned|Q_2: p16|||Part of Cover Sequence 3 (1690-1650 Ma) of the Eastern Fold Belt, Mount Isa Inlier.||||||
16404|Roxmere Quartzite|68732|6|Mentioned|p165 Fig.3, p167|Statherian|Statherian|Of the Prize Supersequence. Maximum sedimentary depositional ages.|1712 +/- 4, 1713 +/- 6 Ma|||||
16404|Roxmere Quartzite|69056|5|Briefly described|p2, p54|Statherian|Statherian|See also Time-Space plot sheet, Reference images sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Staveley Formation. Maximum depositional age.|1713 +/- 6 Ma.|||Gradationally overlies Staveley Formation.|Isolated areas of cross-bedded, fine-grained quartzose to feldspathic sandstone.|
16404|Roxmere Quartzite|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination|
16404|Roxmere Quartzite|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination|
16404|Roxmere Quartzite|69591|4|Described|p29, p38 Fig.2.22, p39, p40 Fig.2.27|Paleoproterozoic|Paleoproterozoic|See also p48-49, p56, p107. Marimo-Staveley and Fig Tree Gully Domains, Calvert Superbasin. Part of the Big Supersequence. Shallow-marine deposits. Large-scale nappes produce alternating upward-facing and downward-facing belts. Detrital zircons aged ~1712 Ma are consistent with derivation from Fiery Creek Volcanics (or equivalents). Shown as not part of the Mount Albert Group on p56.|~1710 Ma (MDA: Carson et al., 2011).|Mount Albert Group [?].||Overlies Staveley Formation gradationally.|Feldspathic sandstone, minor siltstone, rare conglomerate; locally abundant ripple marks and ripple cross-lamination.|
16404|Roxmere Quartzite|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Overlies Staveley Formation.|Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross-lamination.|
16404|Roxmere Quartzite|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Overlies Staveley Formation.|Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross-lamination.|
16404|Roxmere Quartzite|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple-marks and ripple cross-lamination.|
16404|Roxmere Quartzite|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple-marks and ripple cross-lamination.|
16404|Roxmere Quartzite|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Overlies Staveley Formation. Is overlain by Starcross Formation (Kuridala Group).|Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination.|05-MAY-16
16404|Roxmere Quartzite|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.|||Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination.|
16404|Roxmere Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1713+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
16404|Roxmere Quartzite|71799|5|Briefly described|p150 fig 2, p155|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca 1700 Ma|||Overlies the Staveley Formation.|Quartzite, sandstone and greywacke.|
16404|Roxmere Quartzite|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain.||Mount Albert Group||Overlies Staveley Formation.|Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination.|
16404|Roxmere Quartzite|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain.||Mount Albert Group||Overlies Staveley Formation.|Feldspathic sandstone, minor siltstone and rare conglomerate; locally abundant ripple marks and ripple cross lamination.|
16404|Roxmere Quartzite|72889|5|Briefly described|p5, p6 Fig.i.|Statherian|Statherian|Maximum depositional age determined by Neumann (Geochron Delivery-b, Withnall, 2019).|c. 1710 Ma.|||Grades transitionally into Staveley Formation in the Marimo area.||
16404|Roxmere Quartzite|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
16404|Roxmere Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Kuridala-Selwyn-Marimo-Doherty Domain.|1713+/-6 Ma maximum depositional age||||Siliciclastics.|
16481|Ruxton Formation|23032|4|Described|p35,36|Tournaisian|Late Devonian|Previously included in Venetia Formation.||||||
16481|Ruxton Formation|23291|6|Mentioned|p37|Devonian|Devonian|Geological Province: Georgetown Region.||||||08-JUL-15
16481|Ruxton Formation|23422|5|Briefly described|p183|Carboniferous|Carboniferous|||||||
16481|Ruxton Formation|23423|5|Briefly described|Plate 8.3e|||Clarke River Group||||||
16481|Ruxton Formation|23424|4|Described|Table 8.1 Fig 8.4 p338.|Early Carboniferous|Late Devonian|Age: Latest Devonian to early Carboniferous (latest Famennian to Tournaisian); conodonts & brachiopods. Intruded by Carboniferous granites & rhyolite domes. Laterally equiv to Venetia Fm. Of Clarke River Gp Clarke River Basin. Overlies Kangaroo Hill Fm(u)||||||05-MAY-15
16481|Ruxton Formation|23430|4|Described|Plate 14.11 + p508|||Lateral equivalent to Venetia Formation. Of Clarke River Group. Camel Creek Subprovince. Clarke River Basin Province.||||||18-JUL-14
16481|Ruxton Formation|23431|5|Briefly described|p542|||Of Clarke River Group||||||
16481|Ruxton Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Clarke River Group.||||||
16481|Ruxton Formation|23893|5|Briefly described|p17|Tournaisian|Famennian|Can be divided into 6 informal subunits. Geological Province: Clarke River Basin.||||||07-JUL-15
16481|Ruxton Formation|24577|4|Described|p751, p752 Fig.1, p754 Fig.2|Tournaisian|Tournaisian|Of the Clarke River Group. Overlain by the Lyall Formation. Geological Province: Camel Creek Region and Clarke River Basin, Lachlan Fold Belt.||||||
16481|Ruxton Formation|24613|5|Briefly described|p9 Fig. 4, p77, p135|Tournaisian|Famennian|Geological province: Burdekin Basin, Clarke River Basin.||||||07-FEB-11
16481|Ruxton Formation|24614|5|Briefly described|p191 Fig. 1|||Of Clarke River Group. Sandstone-mudstone sequence with a thickness of 750m. Geological Province: Clarke River Province. See also p201 Fig. 8.||||||07-FEB-11
16481|Ruxton Formation|42690|5|Briefly described|map legend|Carboniferous||||||||
16481|Ruxton Formation|42692|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
16481|Ruxton Formation|42933|2|Defined|p208|Early Carboniferous||of Clarke River Group||||||
16481|Ruxton Formation|43095|5|Briefly described|Plate 2|||of Clarke River Group||||||
16481|Ruxton Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Clarke River Group.||||||
16481|Ruxton Formation|67402|4|Described|p239, p244, p245 fig BND/CLR3|Tournaisian|Famennian|Clarke River Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under alluvial fan, alluvial plain or shelf conditions. Maximum thickness of 750m.||Clarke River Group||Equivalent to the Ruxton Formation. Overlain by the Lyall Formation.|Quartzose to feldspathic sandstone and conglomerate, siltstone, mudstone, local calcareous sandstone and limestone, minor tuffaceous siltstone.|
16481|Ruxton Formation|68339|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and shale; local fine-grained calcareous sandstone, siltstone, shale and impure limestone with marine fossils.|
16481|Ruxton Formation|68340|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Clarke River Basin.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and shale; local fine-grained calcareous sandstone, siltstone, shale and impure limestone with marine fossils.|
16481|Ruxton Formation|68350|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin. Has low K, Th and U radiometric responses.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and shale; local fine-grained calcareous sandstone, siltstone, shale and impure limestone with marine fossils.|
16481|Ruxton Formation|68351|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Burdekin Basin. Has low K, Th and U radiometric responses.||Unit in Clarke River Group.|||Quartzose to feldspathic sandstone and conglomerate, siltstone and shale; local fine-grained calcareous sandstone, siltstone, shale and impure limestone with marine fossils.|
16481|Ruxton Formation|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
16481|Ruxton Formation|68731|6|Mentioned|p203|Mississippian|Mississippian|||||Unconformably overlain by the Hells Gate Rhyolite.||
16481|Ruxton Formation|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Clarke River Basin, Broken River Province.||Clarke River Group.||||
16481|Ruxton Formation|69591|6|Mentioned|p103|Famennian|Famennian|Draper, Scott and Withnall (1993).||||||
16481|Ruxton Formation|69592|5|Briefly described|p274 Fig.4.65, p275|Tournaisian|Tournaisian|Clarke River Basin. Exposed in the Blue Range. Up to 750m thick. Overlaps in age with Venetia Formation. The basal conglomerate, with clasts from the underlying Kangaroo Hills Formation, had previously been excluded from this unit by Draper, Scott and Withnall (1993). Shallow-marine to deltaic deposits.||Clarke River Group.|||Mainly medium- to very fine-grained micaceous sandstone with subordinate siltstone and mudstone; diverse shelly fossils are characteristic. Basal, massive, red pebble to cobble conglomerate and coarse-grained quartzose sandstone.|
16520|Saint Anns Formation|22675|4|Described|p23|Early Carboniferous|Late Devonian|Drummond Basin||||||
16520|Saint Anns Formation|22800|3|Fully described|Fig.14 p592, p580|Tournaisian|Famennian|Spelt St Anns Formation. See also p582, Fig.3 p582||||||
16520|Saint Anns Formation|23052|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
16520|Saint Anns Formation|23161|4|Described|p13 table2a|Early Carboniferous|Late Devonian|||||||
16520|Saint Anns Formation|23430|4|Described|p510|||Drummond Basin Province||||||
16520|Saint Anns Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Late Devonian|Rhyolite, tuff and algal limestone; minor lithic sandstone, conglomerate, siltstone and mudstone.  Max. thickness: 2100m.  Geological Province: Drummond Basin.||||||
16520|Saint Anns Formation|30151|4|Described|p13|||Upper Devonian? - Lower Carboniferous. See also Fig.3.||||||
16520|Saint Anns Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
16520|Saint Anns Formation|31984|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian to Lower Carboniferous||||||
16520|Saint Anns Formation|31999|5|Briefly described|p136|||Table 1||||||
16520|Saint Anns Formation|32490|4|Described|Table 1|||U.Dev.-L.Carb.||||||
16520|Saint Anns Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|U.Dev.-L.Carb.||||||
16520|Saint Anns Formation|32553|4|Described|p46|||||||||
16520|Saint Anns Formation|32556|4|Described|Table 2|||U.Dev.-L.Carb.||||||
16520|Saint Anns Formation|32865|4|Described|p482|||Late Dev. - early Carb.||||||
16520|Saint Anns Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Middle Devonian|Middle Devonian to Lower Carboniferous||||||
16520|Saint Anns Formation|33641|6|Mentioned|p59|||||||||
16520|Saint Anns Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
16520|Saint Anns Formation|34408|6|Mentioned|p185|||On table||||||
16520|Saint Anns Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
16520|Saint Anns Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Early Carboniferous to Late Devonian||||||
16520|Saint Anns Formation|37565|6|Mentioned|Fig.8|||||||||
16520|Saint Anns Formation|37573|4|Described|Table 2|||See also Fig.2||||||
16520|Saint Anns Formation|39445|5|Briefly described|Table 6|||||||||
16520|Saint Anns Formation|41246|6|Mentioned|Map legend|Devonian||||||||
16520|Saint Anns Formation|41639|6|Mentioned|p7|||||||||
16520|Saint Anns Formation|42486|5|Briefly described|p201|||||||||
16520|Saint Anns Formation|42547|5|Briefly described|p60|||||||||
16520|Saint Anns Formation|42701|4|Described|p24|||Actually spelt St Anns Formation||||||
16520|Saint Anns Formation|43103|6|Mentioned|p19|||actually spelt St Anns Formation.||||||
16520|Saint Anns Formation|43104|5|Briefly described|p54|||actually spelt St Anns Formation||||||
16520|Saint Anns Formation|43105|5|Briefly described|p12|||||||||
16520|Saint Anns Formation|43213|6|Mentioned|p67, p74|Late Devonian|Late Devonian|Among the oldest rocks in north Drummond Basin.||||||
16520|Saint Anns Formation|43391|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Geological Province: Drummond Basin.  Mainly mudstone, sandstone, and conglomerate; minor limestone; rare ignimbrite.||||||23-JUN-04
16520|Saint Anns Formation|43706|5|Briefly described|p12|Early Carboniferous|Late Devonian|||||||
16520|Saint Anns Formation|44245|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
16520|Saint Anns Formation|45073|6|Mentioned|p63|||U.Dev.-L.Carb. Phosphate.||||||
16520|Saint Anns Formation|45151|5|Briefly described|Table 6|||||||||
16520|Saint Anns Formation|48914|6|Mentioned|p31|||U.Dev. - L.Carb.||||||
16520|Saint Anns Formation|48922|4|Described|p13|||||||||
16520|Saint Anns Formation|60659|4|Described|p12, p62, p64 Fig. 6|||Includes Llanarth Vol Mbr. Unconformable on Anakie Metamorphic Gp + Ukalunda beds; conformably overlain; Scartwater Fm; also overlain by Stones Creek Vols. Intruded by  Sunbeam Granodiorite. Geol.Prov: Drummond Basin.||||||07-FEB-11
16520|Saint Anns Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Contains Llanarth Member. Sandstone, siltstone, shale, coarse feldspathic sandstone, algal limestone pods, minor volcanics; plus volcaniclastic sandstone/siltstone member, with unnamed basalt + andesite flows interbedded with volcanolithic arenite/rudite.||||||10-FEB-09
16520|Saint Anns Formation|64852|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Sandstone, siltstone, shale, coarse feldspathic sandstone, algal limestone pods, minor volcanics; and an unnamed subunit of basalt and andesite flows interbedded with volcanolithic arenite and rudite.||||||10-FEB-09
16520|Saint Anns Formation|66188|6|Mentioned|443, Fig 3, Fig 16-17|Early Carboniferous|Late Devonian|Of the Drummond Basin||||||
16520|Saint Anns Formation|67402|4|Described|p196 fig DRM2, p197, p201|Tournaisian|Famennian|Drummond Basin. Deposited in a near-shore or marine environment. Approximately 200m thick.||||Unconformably overlies the Mount Wyatt beds. Overlain by the Scartwater Formation.|Basal conglomerate, followed by interbedded lithic sandstone, tuffaceous sandstone, siltstone, mudstone and limestone.|
16520|Saint Anns Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Drummond Basin. This unit, as well as the Bimurra, Foyle, Silver Hills and Stones Creek Volcanics, and the Mount Wyatt Formation, are all mapped under the symbol, DCD1.||||||
16520|Saint Anns Formation|68679|6|Mentioned|p364|Early Carboniferous|Late Devonian|Thomson Orogen.||||||
16520|Saint Anns Formation|68731|5|Briefly described|p128, p132, p191, p192, p193 Fig 3.106|Early Carboniferous|Late Devonian|Anakie Inlier. Contains sandstone that is sporadically cross-laminated and contains local pebbly horizons and mudstone with sporadically developed mudcracks; uncommon intervals of tuff and ignimbrite and rare horizons of chert also occur.|||Includes the Llanarth Volcanic Member.|Unconformably overlies Les Jumelles beds. Underlain by the Coquelicot Tonalite. Conformably underlain by the Mount Wyatt Formation.|Comprises variably developed, pebble to boulder, basal conglomerate, volcaniclastic sandstone, as well as siltstone and mudstone.|11-MAY-16
16520|Saint Anns Formation|68900|3|Fully described|p4, p18, p20, p37-p39, p41-p44|Early Carboniferous|Late Devonian|Drummond Basin. Restricted to the eastern part of the HARVEST HOME and SCARTWATER sheet areas. This unit does not crop out well and produces recessive topography. This unit produces a slightly elevated K signature in airborne radiometric images. According to Olgers (1972) in the type area this unit 2100m thick.Lithology and structure are discussed in detail. Deposited in a near-shore, shallow marine or paralic environment. Probably a time equivalent of the Mount Wyatt Formation and Silver Hills Volcanics. See also p49, p52, p62.|||Includes the Llanarth Volcanic Member.|Unconformably overlies the Les Jumelles beds and the Coquelicot Tonalite. Overlies the Mount Wyatt Formation (probably gradationally). Conformably overlain by the Scartwater Formation.|Red-purple, clast supported, granule to pebble conglomerate that is medium to thick-bedded. Fine to medium-grained and lithic sandstone, oolitic and algal limestones and volcaniclastic sandstones and siltstones.|
16520|Saint Anns Formation|68901|5|Briefly described|p2, p114|Early Carboniferous|Late Devonian|Drummond Basin.||||Overlain by the Pyramid Rhyolite.||27-SEP-18
16520|Saint Anns Formation|69952|6|Mentioned|p85|Early Carboniferous|Late Devonian|Thomson Orogen.||||||
16520|Saint Anns Formation|70740|5|Briefly described|p1, p2, p7, p20, p22, p41|Late Devonian|Late Devonian|Drummond Basin. Possibly extends into the early Carboniferous. Overlain by the Scartwater Formation, Pyramid Rhyolite and the Star of Hope Formation. Equivalent to the Bimurra Volcanics. Partly equivalent to the Mount Wyatt Formation, Silver Hills Volcanics and Stones Creek Volcanics. Intruded by the Rockpool Granite. See also p44, p47-p48, p50, p76, p80-p81, p88, p124, p129.||||Unconformably overlies the Les Jumelles beds and the Coquelicot Tonalite. Conformably overlies the Mount Wyatt Formation.|Conglomerate and sandstones grading into volcaniclastic feldspatholithic and lithofeldspathic sandstones, siltstones and some basaltic lava flows and possible sills.|
16520|Saint Anns Formation|71592|5|Briefly described|Appendix A.|||Drummond Basin.|||||Ignimbrite.|
16520|Saint Anns Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Late Devonian|Geological province: northern Drummond Basin. Written as St Anns Formation.||||Overlain by Scartwater Formation.||
16520|Saint Anns Formation|73035|5|Briefly described|Map legend|Early Carboniferous|Late Devonian||||||Sandstone, siltstone, shale, coarse-grained feldspathic sandstone, algal limestone pods, minor volcanics.|
16520|Saint Anns Formation|73198|4|Described|p499-500, p502, p509-511, p514|||[Written as St Ann's Formation]. Drummond Basin, north. Part of Cycle 1 of Olgers (1972). Records basin-wide contemporaneous volcanism. Maximum thickness: 2100 m. Volcanic provenance. [See article for petrographic descriptions and data].|||Llanarth Volcanic Member|Underlain by Mount Wyatt Formation. Overlain by Scartwater Formation. Equivalent to Silver Hills Volcanics.|Includes thick-bedded to massive dacitic and rhyolitic crystal-rich and crystal poor ignimbrite and tuff with minor dacitic and rhyolitic lavas, and volcanolithic conglomerates, sandstones and siltstones.|
16575|Samford Granodiorite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
16575|Samford Granodiorite|32610|6|Mentioned|p42|||Refers Gradwell (1955)||||||
16575|Samford Granodiorite|33289|4|Described|p163|||Triassic. K/Ar age. See also pp164-166.||||||10-NOV-15
16575|Samford Granodiorite|33381|6|Mentioned|p107|||||||||
16575|Samford Granodiorite|33881|6|Mentioned|p95|||Posibility to be quarried||||||
16575|Samford Granodiorite|35007|6|Mentioned|p74|||||||||
16575|Samford Granodiorite|35063|6|Mentioned|p79|||||||||
16575|Samford Granodiorite|35812|6|Mentioned|p568|||See also Fig.2||||||
16575|Samford Granodiorite|36238|6|Mentioned|Table 1|||||||||
16575|Samford Granodiorite|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early Triassic.||||||10-NOV-15
16575|Samford Granodiorite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
16575|Samford Granodiorite|38074|6|Mentioned|Table 2|||||||||
16575|Samford Granodiorite|39079|6|Mentioned|p9|||||||||
16575|Samford Granodiorite|39445|5|Briefly described|Table 12|||||||||
16575|Samford Granodiorite|40623|5|Briefly described|p20|||||||||
16575|Samford Granodiorite|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
16575|Samford Granodiorite|43008|5|Briefly described|map legend|||||||||
16575|Samford Granodiorite|43009|5|Briefly described|Map Legend|||||||||
16575|Samford Granodiorite|43076|5|Briefly described|p6|||||||||
16575|Samford Granodiorite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
16575|Samford Granodiorite|68576|5|Briefly described|QLD_D1: p7, p17|||Camp Mountain. Map location. Used for the base of Brisbane City Hall.|||||Grey biotite granodiorite with common mafic microdiorite enclaves.|
16575|Samford Granodiorite|68679|5|Briefly described|p334, p427-428, p472|Late Triassic|Late Triassic|Northern New England Orogen; Brisbane area.|225.7 Ma (K-Ar: Green, 1975).|||Intrudes Bunya Phyllite and Neranleigh-Fernvale beds.|Hornblende-biotite granodiorite, quartz diorite and trondhjemite.|
16575|Samford Granodiorite|69952|5|Briefly described|p38|||||||Intrudes Neranleigh-Fernvale beds and Bunya Phyllite.||
16575|Samford Granodiorite|72297|6|Mentioned|p726|||Source of dimension stone; quarried at Samford.||||||
16588|Sandalwood Serpentinite|23032|4|Described|p12|||||||||
16588|Sandalwood Serpentinite|23291|5|Briefly described|p30|Early Paleozoic|Proterozoic|Parent: Boiler Gully Complex. Geological Province: Georgetown Region.||||||08-JUL-15
16588|Sandalwood Serpentinite|23494|5|Briefly described|p10, p24 Tb. 1|Precambrian|Precambrian|Ultrabasic rocks.  Intruded by McKinnons Creek Granite.  Geological Province: Georgetown Inlier.||||||
16588|Sandalwood Serpentinite|23498|5|Briefly described|p25 table 1||Proterozoic|Intruded by McKinnons Creek Granite. Intrudes Lucky Creek Formation and Paddys Creek Formation||||||
16588|Sandalwood Serpentinite|23503|5|Briefly described|Map Legend||Mesoproterozoic|||||||
16588|Sandalwood Serpentinite|23616|5|Briefly described|Table 1C p16, p27.||Proterozoic|Age: Inferred to be Early or Middle Proterozoic. Inferred to be of a similar age to surrounding Halls Reward Metamorphics, but contact between the two may be either conformable, intrusive or tectonic. Hodgkinson Province.||||||
16588|Sandalwood Serpentinite|23619|4|Described|p43 Table 2||Proterozoic|Originally thought to be older than Boiler Gully Complex. Georgetown Province.||||||
16588|Sandalwood Serpentinite|29445|6|Mentioned|p77|||||||||
16588|Sandalwood Serpentinite|30334|6|Mentioned|Table 111|||||||||
16588|Sandalwood Serpentinite|30780|6|Mentioned|p996|||||||||
16588|Sandalwood Serpentinite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16588|Sandalwood Serpentinite|31832|6|Mentioned|Table 6|||||||||
16588|Sandalwood Serpentinite|31999|6|Mentioned|p139|||Permian||||||
16588|Sandalwood Serpentinite|32553|4|Described|p66|||||||||
16588|Sandalwood Serpentinite|32959|6|Mentioned|Fig.30|||||||||
16588|Sandalwood Serpentinite|34013|6|Mentioned|Fig.1|||Proterozoic||||||
16588|Sandalwood Serpentinite|37570|6|Mentioned|p112|||||||||
16588|Sandalwood Serpentinite|39027|6|Mentioned|Map legend|Proterozoic|Proterozoic|Prob. Proterozoic||||||
16588|Sandalwood Serpentinite|39445|6|Mentioned|p45|||See also P56 & Table 3||||||
16588|Sandalwood Serpentinite|39689|6|Mentioned|p49|||||||||
16588|Sandalwood Serpentinite|41594|5|Briefly described|p74|||||||||
16588|Sandalwood Serpentinite|41675|4|Described|p17|||||||||
16588|Sandalwood Serpentinite|42692|5|Briefly described|map legend|Proterozoic||||||||
16588|Sandalwood Serpentinite|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
16588|Sandalwood Serpentinite|43060|5|Briefly described|p34|||||||||
16588|Sandalwood Serpentinite|43113|4|Described|Table 2 p28||Proterozoic|of Boiler Gully Complex||||||
16588|Sandalwood Serpentinite|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age. Of Boiler Gully Complex.||||||
16588|Sandalwood Serpentinite|43286|5|Briefly described|Map Legend||Proterozoic|of Boiler Gully Complex.||||||
16588|Sandalwood Serpentinite|43716|6|Mentioned|p128|||||||||
16588|Sandalwood Serpentinite|43896|14|Not recorded|Map Legend||Proterozoic|||||||
16588|Sandalwood Serpentinite|44043|14|Not recorded|Tb.1,Fig.8,p69-70,74|||Intrudes Halls Reward Metamorphics and probably Paddys Creek Formation.||||||
16588|Sandalwood Serpentinite|44044|14|Not recorded|p125,Fig.18|||||||||
16588|Sandalwood Serpentinite|44048|14|Not recorded|Map Legend||Proterozoic|||||||
16588|Sandalwood Serpentinite|44049|14|Not recorded|Map Legend||Proterozoic|||||||
16588|Sandalwood Serpentinite|44059|2|Defined|p442,445,446|||Pre-Early Silurian? Late Precambrian?||||||
16588|Sandalwood Serpentinite|44246|5|Briefly described|Map Legend||Proterozoic|||||||
16588|Sandalwood Serpentinite|44296|14|Not recorded|Map Legend||Proterozoic|||||||
16588|Sandalwood Serpentinite|44632|14|Not recorded|p79|||||||||
16588|Sandalwood Serpentinite|45009|2|Defined|p21,26,50,75,77,79,|||p80,87,89-90,111,Pl.13,15||||||
16588|Sandalwood Serpentinite|45025|14|Not recorded|p25||Precambrian|Similar serpentine to p25||||||
16588|Sandalwood Serpentinite|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|Of the Boiler Gully Complex.  Serpentinite; minor clinopyroxenite and metagabbro.||||||07-NOV-08
16588|Sandalwood Serpentinite|67455|5|Briefly described|p575 Table 1, pp591-592.|||Halls Reward domain, Greenvale Province. May represent oceanic crust.||Unit in Boiler Gully Complex.|||Metagabbro, interbedded with layered amphibolite of Stenhouse Creek Amphibolite.|
16588|Sandalwood Serpentinite|68336|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.||Unit in Boiler Gully Complex.|||Serpentinite; minor clinopyroxenite and metagabbro.|
16588|Sandalwood Serpentinite|68341|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.||Unit in Boiler Gully Complex.|||Serpentinite; minor clinopyroxenite and metagabbro.|
16588|Sandalwood Serpentinite|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Cape River Province.||Unit in Boiler Gully Complex.|||Serpentinite; minor clinopyroxenite and metagabbro.|
16588|Sandalwood Serpentinite|68731|5|Briefly described|p156|Cambrian|Cambrian|These mafic and ultramafic rocks have been affected by the same metamorphism and deformation as the Halls Reward Metamorphics and are thus likely to be early Paleozoic.  Age further constrained by the Boiler Gully Complex.||Of the Boiler Gully Complex.|||Typically massive with lizardite, chrysotile and antigorite.|
16588|Sandalwood Serpentinite|72297|5|Briefly described|p702|||Part of a narrow belt extending SW from Greenvale.|||||Serpentinised ultrabasics; contains chromite prospects.|
16611|Sandy Creek Gabbro|41659|6|Mentioned|Fig.1|||||||||
16643|Sawmill Coal Member|36825|6|Mentioned|p2|||||||||
16643|Sawmill Coal Member|38310|6|Mentioned|p237|||||||||
16644|Sawmill Seam|36825|6|Mentioned|p2|||||||||
16644|Sawmill Seam|68679|6|Mentioned|p398|Late Triassic|Late Triassic|Informal subdivision of the coal measures (Reid 1945, 1947; Dear, McKellar & Tucker 1971; Flood 1985) recognised a basal conglomerate followed above by the Bottom, Sawmill, Callide and Marker seams.||Callide Coal Measures.||||30-APR-19
16667|Scartwater Formation|22675|4|Described|p33|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
16667|Scartwater Formation|22800|6|Mentioned|Fig.4 p583|||||||||
16667|Scartwater Formation|23161|6|Mentioned|p13|||||||||
16667|Scartwater Formation|23430|6|Mentioned|p510|||||||||
16667|Scartwater Formation|23504|5|Briefly described|Map Legend||Carboniferous|||||||
16667|Scartwater Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Late Devonian|Feldspathic and lithic sandstone, mudstone, tiff and algal limestone.  Max. thickness: 1200m.  Geological Province: Drummond Basin.||||||
16667|Scartwater Formation|30151|6|Mentioned|p13|||Upper Devonian? - Lower Carboniferous.||||||
16667|Scartwater Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
16667|Scartwater Formation|31984|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16667|Scartwater Formation|32490|4|Described|Table 1|||U.Dev.-L.Carb.||||||
16667|Scartwater Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16667|Scartwater Formation|32553|4|Described|p48|||||||||
16667|Scartwater Formation|32556|4|Described|Table 2|||L.Carb.||||||
16667|Scartwater Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
16667|Scartwater Formation|34408|6|Mentioned|p185|||On table||||||
16667|Scartwater Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16667|Scartwater Formation|35811|6|Mentioned|Fig.3|||||||||
16667|Scartwater Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16667|Scartwater Formation|37573|4|Described|Table 2|||||||||
16667|Scartwater Formation|38666|6|Mentioned|p4|||||||||
16667|Scartwater Formation|39445|5|Briefly described|Table 6|||||||||
16667|Scartwater Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
16667|Scartwater Formation|41710|6|Mentioned|Fig.2|||||||||
16667|Scartwater Formation|41805|6|Mentioned|Fig.2|||||||||
16667|Scartwater Formation|42486|5|Briefly described|p201|||||||||
16667|Scartwater Formation|42547|5|Briefly described|Fig.17 P61|||||||||
16667|Scartwater Formation|42701|6|Mentioned|Table 1, P.19|||Old stratigraphic term. Name not used in this eastern sub-basin part of the Drummond Basin.||||||
16667|Scartwater Formation|43093|6|Mentioned|Appendix 1|||mentioned in terms of relationship to Camp Oven Mountain Complex.||||||
16667|Scartwater Formation|43391|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Geological Province: Drummond Basin.  Mainly sandstone and conglomerate.||||||23-JUN-04
16667|Scartwater Formation|43706|5|Briefly described|p12|Early Carboniferous|Early Carboniferous|||||||
16667|Scartwater Formation|43936|5|Briefly described|Map Legend||Carboniferous|||||||
16667|Scartwater Formation|44081|14|Not recorded|p107,109,113,120,|||Fig.6,165,187. Described in French.||||||
16667|Scartwater Formation|45073|6|Mentioned|p26|||Stratigraphy||||||
16667|Scartwater Formation|45151|5|Briefly described|Table 6|||||||||
16667|Scartwater Formation|48914|5|Briefly described|p35|||U.Dev. or L.Carb.  P26.||||||
16667|Scartwater Formation|48922|4|Described|p12|||||||||
16667|Scartwater Formation|60659|4|Described|p13|Early Carboniferous|Early Carboniferous|Interbedded quartz sandstone, mudstone + algal limestone. Overlies Stones Creek Volcanics + Saint Anns Formation; overlain; Mount Hall Formation; unconformably beneath Mount Wickham Rhyolite also. Geol Prov: Drummond Basin.||||||07-FEB-11
16667|Scartwater Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Mudstone, quartzose to feldspathic sublabile sandstone, limestone, tuff and conglomerate.||||||
16667|Scartwater Formation|64852|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Mudstone, quartzose to feldspathic sublabile sandstone, limestone, tuff, conglomerate.||||||
16667|Scartwater Formation|66188|6|Mentioned|Fig 3, TB1, Fig 7-8, Fig 16-17|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
16667|Scartwater Formation|67402|5|Briefly described|p165 tbl LPB1, p196 fig DRM2, p197, p201|Tournaisian|Tournaisian|Drummond Basin. Deposited on a floodplain. Approximately 420m thick.||||Overlies the Saint Anns Formation. Overlain by the Mount Hall Formation.|Interbedded quartz sandstone, mudstone, siltstone and algal limestone with sub-ordinate beds of limestone conglomerate, tuff and lithic sandstone.|
16667|Scartwater Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Mount Hall and Telemon Formations and Raymond Sandstone, are all mapped under the symbol, Cd2.||||||
16667|Scartwater Formation|68679|6|Mentioned|p364|Carboniferous|Carboniferous|Thomson Orogen.||||||
16667|Scartwater Formation|68731|5|Briefly described|p191 Fig 3.102, p193|Mississippian|Mississippian|Drummond Basin. < 1200 m thick. Interpreted alluvial flood plain facies assemblage, subject to periodic pedogenic redbed development. Contains locally abundant and diverse Mississippian lepidodendroid macroflora (White cited in Olgers 1972).|||||Comprises mainly quartzose sandstone interbedded with mudstone and siltstone, with subordinate lacustrine algal limestone, volcanolithic sandstone, tuff and rare conglomerate.|18-JUL-14
16667|Scartwater Formation|68900|2|Defined|p4, p37, p43, p54-p55, p57-p62, p64, p70|Carboniferous|Carboniferous|Drummond Basin. Originally introduced by de Bretizel (1966) for rocks between the Saint Anns Formation and Mount Hall Formation. This unit is confined to the northern Drummond Basin and the type area is 16km south of Scartwater homestead. This unit generally produces recessive topography, particularly compared to units like the Mount Hall Formation. This unit has a low potassium enrichment in airborne raidometric images and in the north of the units distribution in HARVEST HOME it has a faint whitish signature suggesting enrichment in U and Thu. This unit produces a very low magnetic response. Lithology and biostratigraphy are discussed in detail. Sandstones are interpreted as probably fluvial in origin, Van Heeswjick (2006) interpreted an alluvial flood plain facies assemblage. According to Olgers (1972) this unit has a thickness of 1200m in the type area but thins out to 300m thick in the Burdekin River area. Nominally equivalent to the Telemon Formation.||||Overlies the Saint Anns Formation and Stones Creek Volcanics (conformably or disconformably). Conformably overlain by the Mount Hall Formation.|Dominantly massive- to thin-bedded mudstone and siltstone containing calcareous nodules that is interlayered with  lesser quartzose sandstone that is thin- to medium-bedded and very fine- to medium-grained.|
16667|Scartwater Formation|68901|6|Mentioned|p2 Fig. i|Carboniferous|Carboniferous|Drummond Basin.||||||27-SEP-18
16667|Scartwater Formation|69952|6|Mentioned|p85|Carboniferous|Carboniferous|Thomson Orogen.||||||
16667|Scartwater Formation|70740|5|Briefly described|p2, p7, p42, |Early Carboniferous|Early Carboniferous|Drummond Basin. Age based on rich lycopod fossil assemblage. See also p80, p81, p84, p106, p125, p129.||||Overlies the Stones Creek Volcanics and the Saint Anns Formation. Overlain by the Star of Hope Formation. Intruded by the Rockpool Granite.|Mudstone, siltstone with calcareous nodules and sandstones.|
16667|Scartwater Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Early Carboniferous|Geological province: northern Drummond Basin.||||Overlain by Mount Hall Formation. Underlain by St Anns Formation.||
16667|Scartwater Formation|73198|4|Described|p499-500, p502-504, p507, p510-512, p514|||Drummond Basin, north. Part of Cycle 2 of Olgers (1972). Maximum thickness: 1200 m. More lithic rich / less quartz than the equivalent Telemon Formation and contains more tuff and ignimbrite horizons. Basement provenance [also reported as mixed cratonic and volcanic provenance]. [See article for petrographic descriptions and data].||||Underlain by Llanarth Volcanic Member (Saint Anns Formation). Conformably overlain by Mount Hall Formation. Equivalent to Telemon Formation.|Dominated by locally variable cross-bedded and sometimes ripple cross-laminated or horizontally bedded sandstones, siltstones, microbial limestone, minor conglomerates and sparse tuff.|
16691|Scottville Member|23161|4|Described|p30|Early Permian|Early Permian|||||||
16691|Scottville Member|29735|6|Mentioned|Fig.2|||||||||
16691|Scottville Member|32949|2|Defined|p441|Permian|Permian|Refers Malone et al. (1966)||||||
16691|Scottville Member|35150|6|Mentioned|p422|||||||||
16691|Scottville Member|35160|6|Mentioned|p2|||||||||
16691|Scottville Member|36739|6|Mentioned|p8|||||||||
16691|Scottville Member|39212|5|Briefly described|p11|||||||||
16691|Scottville Member|39267|4|Described|p236|||||||||
16691|Scottville Member|39423|6|Mentioned|p60|||||||||
16691|Scottville Member|40093|6|Mentioned|p40|||||||||
16691|Scottville Member|40749|6|Mentioned|Fig.1|||||||||
16691|Scottville Member|41034|6|Mentioned|p367|||||||||
16691|Scottville Member|41666|6|Mentioned|p25|||||||||
16691|Scottville Member|42257|5|Briefly described|Table 1 P263|||||||||
16691|Scottville Member|42701|4|Described|p66|||||||||
16691|Scottville Member|65388|5|Briefly described|p189, 190|Kazanian|Kazanian|Of Blenheim Formation of Runnegar & McClung (1973). Previously "Big Strophalosia Bed". Coquinite. Includes Wyndhamia clarkei assemblage.||||||
16704|Seaforth Microgranite|23042|6|Mentioned|p105|||||||||
16704|Seaforth Microgranite|40577|3|Fully described|p57|||||||||
16704|Seaforth Microgranite|40954|6|Mentioned|p133|||||||||
16704|Seaforth Microgranite|61917|5|Briefly described|Map legend|Tertiary|Tertiary|Porphyritic, partly granophyric microgranite with alkali phenocrysts 1-4mm.||||||
16704|Seaforth Microgranite|65388|4|Described|p421, p403 Fig. 135|Oligocene|Oligocene|May be youngest phase of Mount Jukes Intrusive Complex. Several small intrusions of porphyritic, partly granophyric microgranite.||||||
16704|Seaforth Microgranite|69599|5|Briefly described|p634|||Stephenson (1985). Several small intrusions.||Mount Jukes Intrusive Complex.||||
16704|Seaforth Microgranite|73450|4|Described|p45, p72-73|||Forms three or four small bodies near Seaforth. Interpreted as the youngest main phase of the Mount Jukes Intrusive Complex and may be associated with leucocratic porphyritic dykes (Stephenson, 1985).||Mount Jukes Intrusive Complex|||Microgranite with microperthitic feldspar phenocrysts in a partly granophyric groundmass of K-feldspar and quartz.|
16726|Seigal Volcanics|22538|6|Mentioned|P714||Statherian|||||||
16726|Seigal Volcanics|22644|5|Briefly described|p5 Fig. 2|||Geol province McArthur Basin. Underlain by Yiyinti Sandstone.||||||29-NOV-06
16726|Seigal Volcanics|22853|4|Described|5 & 6|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness: 400 m. Overlain by Sly Creek Sandstone.||||||29-NOV-06
16726|Seigal Volcanics|23065|6|Mentioned|15|||Geological province: McArthur Basin. Of the Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|23066|5|Briefly described|p808|||||||||
16726|Seigal Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
16726|Seigal Volcanics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawallah Group.||||||07-NOV-08
16726|Seigal Volcanics|23395|6|Mentioned|p385|||||||||
16726|Seigal Volcanics|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
16726|Seigal Volcanics|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
16726|Seigal Volcanics|23867|5|Briefly described|Fig. 30|||Of Tawallah Group. Correlates with Nungbalgarri Volcanics of the Kombolgie Subgroup (Katherine River Group).||||||
16726|Seigal Volcanics|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
16726|Seigal Volcanics|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group||||||
16726|Seigal Volcanics|24419|5|Briefly described|p13 Fig.5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Geological Province: McArthur Basin; Murphy Province||||||07-NOV-08
16726|Seigal Volcanics|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Mafic. Geological Province: Southern McArthur Basin.||||||
16726|Seigal Volcanics|31421|6|Mentioned|p507|||See also p509.||||||29-NOV-06
16726|Seigal Volcanics|35114|6|Mentioned|p200|||||||||
16726|Seigal Volcanics|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|36012|3|Fully described|Table 2|||See also p11 and p16.||||||29-NOV-06
16726|Seigal Volcanics|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|37568|5|Briefly described|p78|||||||||
16726|Seigal Volcanics|38584|4|Described|p11, p12|||||||||
16726|Seigal Volcanics|38902|6|Mentioned|p28|||||||||
16726|Seigal Volcanics|39445|5|Briefly described|Table 2|||See also p36.||||||29-NOV-06
16726|Seigal Volcanics|39497|6|Mentioned|Fig.4|||||||||
16726|Seigal Volcanics|39685|6|Mentioned|Fig.1|||||||||
16726|Seigal Volcanics|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|40489|6|Mentioned|p89|||||||||
16726|Seigal Volcanics|40491|6|Mentioned|p79|||||||||
16726|Seigal Volcanics|40691|5|Briefly described|p9|||||||||
16726|Seigal Volcanics|40811|6|Mentioned|p318|||||||||
16726|Seigal Volcanics|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|41125|6|Mentioned|p35|||See also fig.21, fig.22.||||||
16726|Seigal Volcanics|41319|6|Mentioned|Fig.1|||||||||
16726|Seigal Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|41721|3|Fully described|p16|||Of Tawallah Group. Represents lower part of Peters Creek Volcanics (as mapped by Roberts et al,1963).Conformably overlie Westmoreland Conglomerate; underlies Mcdermott  Formation.Thickness:1500m. Geol.prov: McArthur Basin. Basalt and tuff; minor sandstone||||||01-AUG-07
16726|Seigal Volcanics|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|42385|4|Described|p5-6|Mesoproterozoic|Mesoproterozoic|Conformable over Yiyintyi Sandstone; underlies Sly Creek Sandstone.  Max. thickness: up to 400m. Typically occur as amygdaloidal basalt flows with fine-grained, chilled bases and vesicular tops.||||||18-SEP-07
16726|Seigal Volcanics|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
16726|Seigal Volcanics|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||||In schematic section, underlies Sly Creek Sandstone; overlies Yiyintyi Sandstone.|Amygdaloidal basalt lava.|11-NOV-11
16726|Seigal Volcanics|42639|4|Described|p8, Table 4 p11|||||||||
16726|Seigal Volcanics|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
16726|Seigal Volcanics|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Basalt lava, amygaloidal and massive, in part hyaloclastic.||||||19-OCT-05
16726|Seigal Volcanics|42812|3|Fully described|p11, Table 3|||Of Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||29-NOV-06
16726|Seigal Volcanics|43036|3|Fully described|p15|||Of the Tawallah Group.||||||29-NOV-06
16726|Seigal Volcanics|43788|6|Mentioned|p14|||||||||
16726|Seigal Volcanics|45162|2|Defined|p14|Proterozoic|Proterozoic|||||||
16726|Seigal Volcanics|45166|5|Briefly described|p28|||||||||
16726|Seigal Volcanics|46804|6|Mentioned|p154|||||||||
16726|Seigal Volcanics|49001|2|Defined|p4|Carpentarian|Carpentarian|||||||
16726|Seigal Volcanics|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Includes Carolina Sandstone Member. Geological Province: McArthur Basin.||||||05-OCT-07
16726|Seigal Volcanics|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Includes Carolina Sandstone Member. Overlain by Sly Creek Sandstone, underlain by Yiyintyi Sandstone and Westmoreland Conglomerate.||||||
16726|Seigal Volcanics|63112|6|Mentioned|p1191 Fig.2, p1192 Tb.1, p1195, p1206 |||Leichhardt Superbasin. One of the mafic rock units that may have been the source of metals in the basin. Age approximated from Fig.2. 300-400 m thick. Mis-spelt as Siegal on p.1206.|c.1775-1780 Ma.||Includes Carolina Sandstone Member.||Amygdaloidal basalt lava; dolerite sills (a lower basalt-dominated one and an upper mixed basalt-sediment one) separated by fine-grained sandstone.|
16726|Seigal Volcanics|63866|5|Briefly described|p54, p56|||||Myally Supersequence||Overlies the Yiyintyi Sandstone. Equivalent to the Eastern Creek Volcanics and the Buddawadda Basalt.|Mafic volcanic rocks with continental tholeiite affinities.|
16726|Seigal Volcanics|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin. Contemporaneous with volcanism in Mount Isa Inlier.|c.1780 Ma|Unit in Tawallah Group.|||Mafic volcanic rocks.|
16726|Seigal Volcanics|64815|6|Mentioned|p4 Fig.2, p5 Fig.3 |||||Of the Tawallah Group.||||
16726|Seigal Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Of the Tawallah Group.|Includes Carolina Sandstone Member.|||
16726|Seigal Volcanics|65228|5|Briefly described|Figs.02, 05-07, 09.|||McArthur Basin.||Unit in Tawallah Group.|Includes Carolina Sandstone Member.|Overlies Yiyintyi Sandstone and Westmoreland Conglomerate. Is overlain by Sly Creek Sandstone and McDermott Formation.||
16726|Seigal Volcanics|65232|6|Mentioned|p9, p8 Fig. 7, p66, App. 2|||Of Tawallah Group. Conformably overlies Westmoreland Conglomerate. Thickness: up to 1600 m. Basalt flows and minor tuff beds and thin interbeds of siltstone and sandstone. Uranium mineralisation. Geol. Prov: McArthur Basin.||||||09-FEB-10
16726|Seigal Volcanics|65337|6|Mentioned|p13.|||Southern McArthur Basin. Some parts of Mitchiebo Volcanics resemble this unit.||||||
16726|Seigal Volcanics|65340|5|Briefly described|p12 Fig.6, p22, 93.|||A flood basalt unit from 0.1 to 1.6 km thick.||Unit in Tawallah Group.|Includes Carolina Sandstone Member.|Overlies Westmoreland Conglomerate and Yiyintyi Sandstone. Is overlain by Sly Creek Sandstone.||23-MAR-18
16726|Seigal Volcanics|66529|5|Briefly described|p20 Fig.7, p21  |||||||Conformably overlies the Westmoreland Conglomerate. Is overlain by Tawallah Group.|Basalt.|
16726|Seigal Volcanics|67057|6|Mentioned|p462.|Paleoproterozoic|Paleoproterozoic||1780 - 1760 Ma.|||||
16726|Seigal Volcanics|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Overlies Westmoreland Conglomerate. Is overlain by McDermott Formation.|Amygdaloidal basalt.|
16726|Seigal Volcanics|67323|4|Described|GIS attrib tbl, Solid Geology Map, p31|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin. Camooweal-Murphy Domain, Mount Isa Inlier.|~1790 Ma.|Tawallah Group.|Carolina Sandstone Member.|Is overlain by Sly Creek Sandstone.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone; sandstone and tuff interbeds with scattered basalt bombs or cobbles.|
16726|Seigal Volcanics|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. 1600 m thick.||Tawallah Group||Conformably overlies Yiyintyi Sandstone or Westmoreland Conglomerate. Overlain by McDermott Formation (conformably).|Altered basic lava flows: massive, amygdaloidal, vesicular, brecciate, haematitic; minor siltstone, feldspathic sandstone.|
16726|Seigal Volcanics|68020|6|Mentioned|p127|||||||Unconformably overlies Westmoreland Conglomerate.||
16726|Seigal Volcanics|69383|5|Briefly described|p48|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Carolina Sandstone Member.||A series of basaltic flows and brecciated volcanic facies; flaggy to massive, fine-grained sandstone.|
16726|Seigal Volcanics|69418|6|Mentioned|p3:19|||McArthur Basin. Hosts U in Westmoreland-Murphy-type deposits (described).||||||12-JUL-16
16726|Seigal Volcanics|69423|5|Briefly described|p8:4 Fig.8.7, 5-6|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Hosts a number of uranium +/- gold occurrences.||Tawallah Group.||||12-JUL-16
16726|Seigal Volcanics|69430|4|Described|p15:3, 10-12, 44, 49-50|||Southern McArthur Basin. 225-1500m thick. Mostly subaerial lava. Upper part is correlated with Sly Creek Sandstone (and Rosie Creek Sandstone Member). Is pierced by a Cu-bearing volcanic plug, and hosts economically insignificant vein-type Cu occurrences. Hosts small U-Au deposits (described in some detail).||Tawallah Group.|Carolina Sandstone Member.|Overlies Westmoreland Conglomerate conformably, and Yiyintyi Sandstone conformably or sharply unconformably [?]. Is overlain conformably by McDermott Formation and Sly Creek Sandstone.|Amygdaloidal basalt flows 5-30m thick; thin siltstone and tuffaceous interbeds in upper part. Includes a prominent sandstone bed (Carolina Sandstone Member). Several feeder dykes are known; is intruded by a plug of volcanic breccia.|12-JUL-16
16726|Seigal Volcanics|69433|5|Briefly described|p18:2, 6|||McArthur Basin. Is lithologically and geochemically indistinguishable from the Mitchiebo Volcanics (Lawn Hill Platform).||Tawallah Group.||Probably equivalent to Peters Creek Volcanics (Lawn Hill Platform). Correlated with Mitchiebo Volcanics.||12-JUL-16
16726|Seigal Volcanics|69591|5|Briefly described|p33-34, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Correlations with Eastern Creek Volcanics and Buddawadda Basalt Member (Peters Creek Volcanics) are speculative.||Tawallah Group.||Overlies Westmoreland Conglomerate.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone; sandstone and tuff interbeds with scattered basalt bombs or cobbles.|
16726|Seigal Volcanics|69673|6|Mentioned|p16 fig 13, p17 fig 14|||||Tawallah Group|Includes Carolina Sandstone Member|Overlain by Sly Creek Sandstone, Rosie Creek Sandstone Member, overlies Yiyintyi Sandstone||
16726|Seigal Volcanics|70284|5|Briefly described|p1244, p1245-1247, p1250-1253, 1257|Statherian|Statherian|McArthur Basin, Leichhardt Superbasin. Generally <20m thick, but may be up to 1600m thick. Geochemistry suggests dolerite dykes in region may be feeders.||||Conformably overlies Westmoreland Conglomerate.|Basaltic lava flows.|14-DEC-16
16726|Seigal Volcanics|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.|Carolina Sandstone Member.|Overlies Westmoreland Conglomerate. Is overlain by McDermott Formation.|Vesicular and amygdaloidal basalt; massive non-vesicular basalt; thin siltstone, sandstone and tuff interbeds.|
16726|Seigal Volcanics|71799|5|Briefly described|p150 fig 2, p156, p157 fig 5, p158|Statherian|Statherian|McArthur Basin.|ca. 1780 Ma|||Overlies the Westmoreland Conglomerate.|Basalt, dolerite, gabbro or amphibolite.|
16726|Seigal Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Tawallah Group||Partially overlies Yiyintyi Sandstone and Westmoreland Conglomerate and partially underlies Rosie Creek Sandstone Member and underlies and is laterally equivalent to Sly Creek Sandstone.||
16726|Seigal Volcanics|72718|6|Mentioned|p7|||Southern McArthur Basin. Incorporates[?] Carolina Sandstone Member.||Tawallah Group|Carolina Sandstone Member|Partly underlain by Yiyintyi Sandstone and Westmoreland Conglomerate. Partly overlain by and equivalent to Sly Creek Sandstone. Partly overlain by Rosie Creek Sandstone Member.||
16726|Seigal Volcanics|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.||Tawallah Group||Overlies Yiyintyi Sandstone and Westmoreland Conglomerate, and underlies Sly Creek Sandstone and Rosie Creek Sandstone Member.||
16726|Seigal Volcanics|72919|6|Mentioned|p12|||[Written as Seigal Volcanics?]. Possibly intersected in drillhole BEN-SD60.|||||May include andesitic volcanics.|
16726|Seigal Volcanics|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.  Partly overlain by Sly Creek Sandstone and Rosie Creek Sandstone Member.||Tawallah Group||Partly underlain by Yiyintyi Sandstone and Westmoreland Conglomerate.||
16726|Seigal Volcanics|73083|6|Mentioned|p35, p77|||||Tawallah Group||||
16726|Seigal Volcanics|73412|5|Briefly described|p2, 4, 8-9, 12, 20|||Southern McArthur Basin. Characterised by a magnetic low; ?reversely magnetised.||Tawallah Group.||Overlies Yiyintyi Sandstone and Westmoreland Conglomerate. Is overlain by Sly Creek Sandstone.||
16734|Sellheim Formation|30148|4|Described|p31|||Pleistocene||||||
16734|Sellheim Formation|30149|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
16734|Sellheim Formation|30151|4|Described|p20|||Table 3 on P20 Pleistocene.||||||
16734|Sellheim Formation|31813|6|Mentioned|p5|||||||||
16734|Sellheim Formation|34409|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
16734|Sellheim Formation|36472|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
16734|Sellheim Formation|37605|6|Mentioned|p380|||||||||
16734|Sellheim Formation|37607|6|Mentioned|Fig.7|||||||||
16734|Sellheim Formation|39445|5|Briefly described|Table 14|||||||||
16734|Sellheim Formation|39730|6|Mentioned|p32|||||||||
16734|Sellheim Formation|41244|6|Mentioned|p31|||||||||
16734|Sellheim Formation|41537|6|Mentioned|Fig.2|||||||||
16734|Sellheim Formation|44060|14|Not recorded|Map Legend|Pleistocene|Pliocene|||||||
16734|Sellheim Formation|44061|4|Described|Table 6|Pleistocene|Pliocene|||||||
16734|Sellheim Formation|48904|2|Defined|p68|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
16734|Sellheim Formation|48914|4|Described|p58|||Pliocene - Pleistocene||||||
16743|Selwyn Range Limestone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Calcilutite, marl, chert. Underlies: O'Hara Shale. Overlies: Devoncourt Limestone.||||||27-AUG-04
16743|Selwyn Range Limestone|22954|6|Mentioned|Fig3p9|Mindyallan|Mindyallan|||||||
16743|Selwyn Range Limestone|24065|5|Briefly described|p234|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 35m.||||||
16743|Selwyn Range Limestone|30479|6|Mentioned|Fig.5|||Stratigraphic relationships||||||
16743|Selwyn Range Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16743|Selwyn Range Limestone|31396|6|Mentioned|Fig.3|||||||||
16743|Selwyn Range Limestone|32952|6|Mentioned|p1188|||See also p1189. Middle - Upper  Cambrian.||||||02-APR-07
16743|Selwyn Range Limestone|33111|4|Described|p42|||||||||
16743|Selwyn Range Limestone|33482|6|Mentioned|Fig.4|||Middle - Upper Cambrian||||||
16743|Selwyn Range Limestone|35054|6|Mentioned|Table 23|||||||||
16743|Selwyn Range Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
16743|Selwyn Range Limestone|35139|4|Described|Table.2|||||||||
16743|Selwyn Range Limestone|37275|6|Mentioned|Fig.1|||||||||
16743|Selwyn Range Limestone|37572|4|Described|p159|||See also p165 and Fig.8.||||||02-APR-07
16743|Selwyn Range Limestone|37816|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
16743|Selwyn Range Limestone|38350|6|Mentioned|p22|||||||||
16743|Selwyn Range Limestone|38444|6|Mentioned|p139|||||||||
16743|Selwyn Range Limestone|38446|6|Mentioned|Table 23|||||||||
16743|Selwyn Range Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
16743|Selwyn Range Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||02-APR-07
16743|Selwyn Range Limestone|39690|6|Mentioned|Fig.2|||||||||
16743|Selwyn Range Limestone|43883|14|Not recorded|p18 Fig.4-3|||||||||
16743|Selwyn Range Limestone|44091|14|Not recorded|p17,Tb.1,p19||Late Cambrian|||||||
16743|Selwyn Range Limestone|44205|14|Not recorded|p9-19,21-28,38-41,||Late Cambrian|p179-185. Replaces Selwyn Limestone.||||||
16743|Selwyn Range Limestone|44211|14|Not recorded|p97,100-107|||Rests between Devoncourt Limestone below and O'Hara Shale above.||||||
16743|Selwyn Range Limestone|44275|14|Not recorded|Map Legend|||||||||
16743|Selwyn Range Limestone|44276|2|Defined|p18,20,21,Tb.2,map|||||||||
16743|Selwyn Range Limestone|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
16743|Selwyn Range Limestone|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
16743|Selwyn Range Limestone|45012|14|Not recorded|p31,32|||||||||
16743|Selwyn Range Limestone|45052|3|Fully described|p102|||See also p32. Middle  or Upper Cambrian.||||||02-APR-07
16743|Selwyn Range Limestone|45079|6|Mentioned|p34|||Cambrian age. Lithology||||||
16743|Selwyn Range Limestone|45166|5|Briefly described|Table 15|||||||||
16743|Selwyn Range Limestone|50100|5|Briefly described|p22|Late Cambrian|Middle Cambrian|Pale flaggy micritic limestone, dolomite and chert layers with marly interbeds.  Rests conformably on Devoncourt Limestone; conformably overlain by Pomegranate Limestone.||||||
16743|Selwyn Range Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Calcilutite, marl; minor chert.||||||
16743|Selwyn Range Limestone|63450|5|Briefly described|p78 Fig. 5|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
16743|Selwyn Range Limestone|64068|4|Described|p70, 62, 64, 65, 69|Late Cambrian|Late Cambrian|Eastern Georgina Basin. Contains trilobites and brachiopods. 30-35 m thick. Correlated with Arthur Creek Formation, Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Mungerebar Limestone. Fauna indicates Late Cambrian (Mindyallan) Glyptagnostus stolidotus Zone in part, but considered by Öpik (1967) to be partly latest Middle Cambrian.||Of Narpa Group.||Laterally interdigitates with and conformably overlies Devoncourt Limestone. Is overlain by, and interdigitates with, O'Hara Shale.|Thin-bedded calcimudstone, marly limestone interbeds; minor dolostone and chert.|21-MAR-16
16743|Selwyn Range Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin.||Narpa Group.||Overlies Devoncourt Limestone. Is overlain by O'Hara Shale.|Calcilutite, marly interbeds, subordinate chert.|
16743|Selwyn Range Limestone|67870|6|Mentioned|p43|Middle Cambrian|Middle Cambrian|Burke River Structural Belt, Georgina Basin.||||||
16743|Selwyn Range Limestone|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
16743|Selwyn Range Limestone|69573|6|Mentioned|p661|||||||||
16743|Selwyn Range Limestone|69591|5|Briefly described|p87, p92-94, p96-97|Cambrian|Cambrian|Burke River Structural Belt, Georgina Basin. About 35m thick. A noticeable feature is limonite pseudomorphs (after pyrite?) but the hopper crystal habit suggests halite. Unfossiliferous.||Narpa Group.||Gradationally overlies Devoncourt Limestone. Is overlain by O'Hara Shale.|Thin-bedded, grey to pink calcilutite with shaly, marly interbeds and a few chert layers; rare cross-bedding.|
16743|Selwyn Range Limestone|72321|6|Mentioned|Fig 2|Guzhangian|Guzhangian|Burke River Structural Belt, Georgina Basin. Australian stages:  Boomerangian to Mindyallan.||of Narpa Group.||||
16743|Selwyn Range Limestone|72516|6|Mentioned|p92-94|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation, Eurowie Sandstone Member and the Arrinthrunga Formation.||03-JUN-21
16743|Selwyn Range Limestone|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Overlies Devonport Limestone and underlies  O'Hara Shale.|Calcilutite with marly interbeds and subordinate chert.|
16743|Selwyn Range Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt.||Narpa Group||Overlies Devoncourt Limestone, Roaring Siltstone, underlies Pomegranate Limestone|Limestone.|
16787|Shady Bore Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
16787|Shady Bore Quartzite|22453|6|Mentioned|p 12|||||||||
16787|Shady Bore Quartzite|22680|6|Mentioned|83,85-87|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23031|6|Mentioned|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23072|5|Briefly described|p754|||||||||
16787|Shady Bore Quartzite|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlies Lady Loretta Formation.||||||07-NOV-08
16787|Shady Bore Quartzite|23396|5|Briefly described|p407 Fig.2|||Of McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23397|5|Briefly described|p471|||||||||
16787|Shady Bore Quartzite|23398|5|Briefly described|p447|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23405|5|Briefly described|p565 Fig.2|||Of McNamara Group.||||||
16787|Shady Bore Quartzite|23406|5|Briefly described|p606|||Of Fickling Group?||||||24-JUN-09
16787|Shady Bore Quartzite|23408|5|Briefly described|p513 Fig.2|||Of McNamara Group||||||30-NOV-06
16787|Shady Bore Quartzite|23409|4|Described|p541|||Of McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
16787|Shady Bore Quartzite|23958|3|Fully described|p1134|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Max. thickness: 460m.||||||07-NOV-08
16787|Shady Bore Quartzite|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thickness: 590m.||||||13-MAY-14
16787|Shady Bore Quartzite|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
16787|Shady Bore Quartzite|24033|6|Mentioned|p25, p26 Fig. 10|||||||||
16787|Shady Bore Quartzite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province: Mount Isa Superbasin.||||||07-NOV-08
16787|Shady Bore Quartzite|24309|5|Briefly described|p1024|Proterozoic|Proterozoic|Of the McNamara Group.||||||30-NOV-06
16787|Shady Bore Quartzite|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlain by Riversleigh Siltstone. Age: c.1647 Ma. Geological Province: Lawn Hill Platform.||||||
16787|Shady Bore Quartzite|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the McNamara Group.  Age: >1590Ma.||||||
16787|Shady Bore Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|36937|6|Mentioned|p229|||||||||
16787|Shady Bore Quartzite|37459|1|Redefined|p431|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||30-NOV-06
16787|Shady Bore Quartzite|37568|5|Briefly described|p84|||||||||
16787|Shady Bore Quartzite|38237|4|Described|p129|||||||||
16787|Shady Bore Quartzite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|38348|4|Described|p13|||||||||
16787|Shady Bore Quartzite|38584|6|Mentioned|p22|||||||||
16787|Shady Bore Quartzite|39445|5|Briefly described|Table 2|||||||||
16787|Shady Bore Quartzite|39497|6|Mentioned|p14|||See also Fig.4||||||
16787|Shady Bore Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Overlies Lady Loretta Formation.||||||15-JUN-06
16787|Shady Bore Quartzite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|39925|6|Mentioned|Fig.9|||||||||
16787|Shady Bore Quartzite|39944|6|Mentioned|Fig.1|||||||||
16787|Shady Bore Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
16787|Shady Bore Quartzite|40221|3|Fully described|p18|||||||||
16787|Shady Bore Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
16787|Shady Bore Quartzite|43486|5|Briefly described|21|||||||||
16787|Shady Bore Quartzite|45166|5|Briefly described|p30|||||||||
16787|Shady Bore Quartzite|47083|4|Described|p18||Proterozoic|Of McNamara Group. Overlain by Riversleigh Siltstone; underlain by Lady Loretta Fm. Maximum thickness: 250 m.||||||30-NOV-06
16787|Shady Bore Quartzite|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: >1644 Ma, <1647 Ma. Conformably overlies Lady Loretta Formation, conformably overlain by Riversleigh Siltstone. Geological Province: Western Fold Belt.||||||19-DEC-07
16787|Shady Bore Quartzite|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  White, flaggy to massive, medium orthoquartzite, siltstone and dolomite.  Overlies Lady Loretta Formation; overlain by Riversleigh Siltstone.||||||28-JUN-04
16787|Shady Bore Quartzite|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Riversleigh Siltstone, underlain by Lady Loretta Formation.||||||
16787|Shady Bore Quartzite|61913|6|Mentioned|p161|||||||||
16787|Shady Bore Quartzite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
16787|Shady Bore Quartzite|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Shady Bore Qzit.||McNamara Group|||Rift phase clastics.|
16787|Shady Bore Quartzite|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Lithology not specified.||McNamara Group.||||
16787|Shady Bore Quartzite|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. White, very fine to medium grained lithic and sublithic sandstone with wave rippled bedding surfaces.||||||
16787|Shady Bore Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Riversleigh Siltstone. Geological Province: Isa Superbasin. Consists of sandstone and conglomerate.||||||30-SEP-08
16787|Shady Bore Quartzite|63111|5|Briefly described|p1162, p1163 Fig. 3|Statherian|Statherian|Of River Supersequence. Age: 1644+/-8 and 1640+/-7Ma. Geological Province: Isa Superbasin. Consists of conglomerates and fine-grained arenites.||||||07-FEB-11
16787|Shady Bore Quartzite|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of River supersequence.|Between 1647 Ma and 1644 Ma.|Of the McNamara Group||Overlies ?unconformably Lady Loretta Formation. Is overlain by Riversleigh Siltstone.||
16787|Shady Bore Quartzite|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Shady Bore.||Of the River supersequence.||Overlies Lady Loretta Formation.||
16787|Shady Bore Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
16787|Shady Bore Quartzite|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed. Basal unit of River supersequence. Shows well-developed quartz cements and stylolites subparallel to bedding; probably an initial aquifer but became an aquiclude early in the history of the basin.||||||
16787|Shady Bore Quartzite|64250|6|Mentioned|p11 fig 3|||||Unit in McNamara Group.||||
16787|Shady Bore Quartzite|64575|6|Mentioned|p665|||||||||
16787|Shady Bore Quartzite|65337|4|Described|p9 Fig.5, pp21-22, p26.|Paleoproterozoic|Paleoproterozoic|Southeast MOUNT DRUMMOND area. Up to 50 m of shallow marine deposits.||Unit in McNamara Group.||Overlies Brumby Formation and Lady Loretta Formation. Is overlain by Plain Creek Formation and Riversleigh Siltstone.|White, very fine- to medium-grained lithic and sublithic sandstone; prominently wave-rippled bedding surfaces.|
16787|Shady Bore Quartzite|65396|5|Briefly described|p82, p175, p241|||Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.||McNamara Group||Overlies Lady Loretta Formation; overlain by Riversleigh Formation.||04-APR-17
16787|Shady Bore Quartzite|66843|6|Mentioned|p38 Fig.10|||shown only as Shady Bore.||||||12-SEP-19
16787|Shady Bore Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also , Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Mount Isa Inlier, Isa Superbasin.||McNamara Group.|||Flaggy to massive medium orthoquartzite; interbeds of fine sandstone, siltstone, and dolomite|
16787|Shady Bore Quartzite|68542|6|Mentioned|p6|||||Upper McNamara Group||Overlain by Riversleigh Siltstone|Basal, coarse clastics fining upwards into a thick sequence of dolomitic siltstone.|
16787|Shady Bore Quartzite|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Upper McNamara Group.||Overlies Lady Loretta Formation. Is overlain by Riversleigh Siltstone.||
16787|Shady Bore Quartzite|68732|6|Mentioned|p165 Fig.3|||Presented as Shady Bore in figure. Of the River Supersequence.||||||
16787|Shady Bore Quartzite|69433|4|Described|p18:2, 5-6, 9|Statherian|Statherian|Southern succession, Lawn Hill Platform. Up to 50m thick. Wave-dominated marine shoreline deposits in a series of upward-shallowing cycles.|c.1640 Ma.|McNamara Group.||Conformably overlies Brumby Formation. Is overlain conformably and transitionally by Plain Creek Formation. Correlative of Breakfast Sandstone (?).|White, thinly to thickly bedded, fine- and medium-grained lithic and sublithic sandstone; features cross-beds and prominent wave ripple marks on bedding surfaces.|12-JUL-16
16787|Shady Bore Quartzite|69591|5|Briefly described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Part of the River Supersequence. High energy fluvial/shallow marine deposits.||McNamara Group.|||Flaggy to massive medium orthoquartzite; interbeds of fine sandstone, siltstone and dolomite.|
16787|Shady Bore Quartzite|69673|5|Briefly described|p52 fig 42, p53 |||40-50m thick. Deposited in a wave dominated marine shoreline environment in a series of upward shallowing cycles.||McNamara Group|||Lithic and sublithic sandstones.|
16787|Shady Bore Quartzite|70864|5|Briefly described|p75, 74 Fig 2|Mesoproterozoic||||McNamara Group|||Quartz sandstone, siltstones and dolomite.|
16787|Shady Bore Quartzite|70897|6|Mentioned|Fig.1.7.7|||Isa Superbasin.||||||
16787|Shady Bore Quartzite|72526|4|Described|p1-2, p4, p7 Tb.1.1, p8, p10-19|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Maximum depositional age reported here from Lawn Hill, Qld sample: 1694+/-17 Ma. Depositional age already constrained by age from tuffs in underlying Lady Loretta Formation. Previous MDA reported  from Mount Drummond, NT: 1635+/-8 Ma (Kositcin and Carson, 2019). Base of unit shown as older in NT than Qld, p8. Qld sample displays bedding surfaces with wave ripples and tabular moulds of probable rip-up mud clasts.See also p85, p87.|1647 Ma to 1635+/-8 Ma.|McNamara Group||Conformably overlies Lady Loretta Formation, Brumby Formation.Conformably underlies Riversleigh Siltstone, Plain Creek Formation.|White very fine to medium-grained sandstone with cross-beds and wave ripples in NT.  Flaggy to massive orthoquartzite with sandstone, some recessive siltstone + dolostone beds,+ with minor mud cracks, mudflake conglomerates + halite casts in QLD.|
16787|Shady Bore Quartzite|72527|4|Described|p1, 7, 8, 105, p112-118, p120, 132, 193|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. 40-50 m thick.  Sampled from Mount Drummond sheet area. Previous geochron sample from Lawn Hill, Qld. See also p194.|1635+/-7 Ma max depositional age|McNamara Group||Conformably overlies Brumby Formation and conformably underlies Plain Creek Formation. Shown as laterally equivalent to Bullrush Conglomerate.|Mapped as massive white fine-grained well-sorted quartzite. Sample is a clean white medium-graned quartz sandstone with rare muscovite.|
16787|Shady Bore Quartzite|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in both Queensland and Northern Territory, but older base in NT. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin.||McNamara Group||Overlies Brumby Formation (NT) and Lady Loretta Formation (Qld) and underlies Plain Creek Formation and is partially equivalent to Bullrush Conglomerate, Mount Les Siltstone and Walford Dolomite.|Includes sandstone.|
16787|Shady Bore Quartzite|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.||McNamara Group||Overlies Lady Loretta Formation and underlies Riversleigh Siltstone.|Includes quartzite, sandstone.|
16787|Shady Bore Quartzite|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Brumby Formation. Overlain by Plain Creek Formation. Equivalent to Bullrush Conglomerate.||
16787|Shady Bore Quartzite|73042|6|Mentioned|p4, p11|Paleoproterozoic|Paleoproterozoic|Mount Isa Province (Lawn Hill Platform) and South Nicholson Basin region, Isa Superbasin. Overlain by Plain Creek Formation.||McNamara Group||Unconformably underlain by Lady Loretta Formation and the Brumby Formation. Conformably overlain by the Riversleigh Siltstone.||
16787|Shady Bore Quartzite|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
16787|Shady Bore Quartzite|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the River Supersequence. Overlies Lady Loretta Formation and overlain by Riversliegh Siltstone, but absent in Lawn Hill Platform area.||||||14-OCT-22
16787|Shady Bore Quartzite|73525|6|Mentioned|p4-5 Fig.2|||Mount Oxide-(Ardmore-May Downs) Domain.|||||Siliciclastics.|
16848|Shoalwater Formation|22740|5|Briefly described|155,156 fig 2, 157|Paleozoic|Paleozoic|Geol province New England Fold Belt. Also on pages 158, 163.||||||07-NOV-08
16848|Shoalwater Formation|23799|6|Mentioned|p25|||Of the Curtis Island Group.  Possible correlative of the Bjelke Petersen beds.||||||
16848|Shoalwater Formation|24382|5|Briefly described|Map legend|Carboniferous|Carboniferous|Parent: Curtis Island Group.||||||18-AUG-08
16848|Shoalwater Formation|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Curtis Island Group.||||||
16848|Shoalwater Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Curtis Island Group.||||||
16848|Shoalwater Formation|24490|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of Curtis Island Group. Quartz arenite, mudstone, schist.||||||04-SEP-08
16848|Shoalwater Formation|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Ccs].  Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.||||||
16848|Shoalwater Formation|30451|5|Briefly described|p8|||||||||
16848|Shoalwater Formation|30777|5|Briefly described|p417|||Discussed||||||
16848|Shoalwater Formation|31657|4|Described|p91|||See also p92. Ordovician - Silurian.||||||30-SEP-08
16848|Shoalwater Formation|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16848|Shoalwater Formation|31659|2|Defined|p17, p18-19|Early Paleozoic|Early Paleozoic|max. thickness: >30,000ft. Quartz greywacke, mudstone, grading in places into schist and gneiss. See also Table 1.||||||07-NOV-08
16848|Shoalwater Formation|32357|4|Described|Table 1|||||||||
16848|Shoalwater Formation|32358|4|Described|Table 1|||||||||
16848|Shoalwater Formation|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16848|Shoalwater Formation|33769|5|Briefly described|p150|||||||||
16848|Shoalwater Formation|33774|6|Mentioned|p6|||Curtis Is. Group. Not recognisable in Mundubbera area.||||||
16848|Shoalwater Formation|36211|6|Mentioned|p269|||||||||
16848|Shoalwater Formation|36488|6|Mentioned|p3|||||||||
16848|Shoalwater Formation|36528|6|Mentioned|p170|||See also Fig.4||||||
16848|Shoalwater Formation|38081|5|Briefly described|Table 1|||||||||
16848|Shoalwater Formation|38143|6|Mentioned|p12|||||||||
16848|Shoalwater Formation|38391|6|Mentioned|p6|||||||||
16848|Shoalwater Formation|38406|5|Briefly described|p9|||||||||
16848|Shoalwater Formation|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous.||||||18-AUG-08
16848|Shoalwater Formation|39445|5|Briefly described|Table 6|||Middle? - Late Carb. See also P83||||||
16848|Shoalwater Formation|40475|6|Mentioned|p2|||||||||
16848|Shoalwater Formation|40960|5|Briefly described|p221|||||||||
16848|Shoalwater Formation|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
16848|Shoalwater Formation|41577|6|Mentioned|Map legend|Late Carboniferous||||||||
16848|Shoalwater Formation|41738|6|Mentioned|p166|||||||||
16848|Shoalwater Formation|41778|6|Mentioned|Table 1|||||||||
16848|Shoalwater Formation|41922|4|Described|Table 1, P11|||||||||
16848|Shoalwater Formation|42547|4|Described|p54|||||||||
16848|Shoalwater Formation|42660|4|Described|p23 p168|||||||||
16848|Shoalwater Formation|42901|6|Mentioned|p403|||||||||
16848|Shoalwater Formation|42980|5|Briefly described|Fig.4,p304|||||||||
16848|Shoalwater Formation|42985|6|Mentioned|p386|||||||||
16848|Shoalwater Formation|43008|5|Briefly described|map legend|||||||||
16848|Shoalwater Formation|43754|3|Fully described|p572-573||Early Carboniferous|||||||
16848|Shoalwater Formation|45107|6|Mentioned|p6|||||||||
16848|Shoalwater Formation|50190|6|Mentioned|p47|||||||||
16848|Shoalwater Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Curtis Island Group.||||||
16848|Shoalwater Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Curtis Island Group||||||
16848|Shoalwater Formation|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Quartzose sandstone, mudstone.||||||
16848|Shoalwater Formation|60557|5|Briefly described|p23|Carboniferous|Devonian|Of the Curtis Island Group. Comprises massive, thick quartz sandstone beds (2-3m thick), with interbedded dark grey to black, thin-bedded to laminated, strongly cleaved phyllitic mudstone.||||||09-JUN-05
16848|Shoalwater Formation|61035|6|Mentioned|p13, p14|Late Carboniferous|Late Carboniferous|Unconformably overlain by Double Mountain Volcanics and Peninsula Range Volcanics. Geological Province: Wandilla Province. Sandstone dominated unit and is also turbiditic in character. Age based on similarities with another unit in Yarrol Province.||||||07-FEB-11
16848|Shoalwater Formation|63821|5|Briefly described|p15, p34, p38|Carboniferous|Carboniferous|Of Curtis Island Group. Max. depositional age: 328.9+/-2.3Ma. Sequence of tightly folded, coarse-grained, quartz-arenite, slate and schist. Geological Province: Wandilla Province - Coastal Block.||||||07-FEB-11
16848|Shoalwater Formation|64556|5|Briefly described|p18|||Of Curtis Island Group. Source of sample material for age analysis was from folded leucocratic biotite microgranite dyke intruding this unit of strongly foliated metasediments.||||||07-FEB-11
16848|Shoalwater Formation|65380|5|Briefly described|p657,658, 660,666-670, 672-674, 676-679|||Coastal Block, New England Orogen. Maximum depositional age from detrital zircon: 327 +/- 1 Ma.|||||Quartz-rich sandstone with only minor volcanics.|27-MAR-12
16848|Shoalwater Formation|65385|6|Mentioned|pS133|||In the New England Orogen. Detrital zircon age of 952+/-9 Ma (Korsch et al., 2009).||||||08-MAR-12
16848|Shoalwater Formation|65452|5|Briefly described|p5-6|Carboniferous|Carboniferous|||||Is overlain by, or faulted against, Agnes Water Volcanics.|Low-grade metasediments.|
16848|Shoalwater Formation|68008|3|Fully described|p110-111, p117-120, p326, p481-482|||Kirkegaard et al. (1970) regarded this as the oldest [sic] unit in the Group. Comprises the Shoalwater terrane. Forms subdued topography with closely spaced dendritic drainage. Structure described. Thickness unknown; the estimated 10,000m of Kirkegaard et al. (1970) ignores its imbricate fault structure as part of an accretionary wedge. The only fossils are unidentifiable flant fragments in black shale. Metamorphosed at 276.8 +/- 4.6 Ma, 274.9 +/- 3.2 Ma (zircon rims: Carson et al., 2006). Other ages discussed.||Topmost Curtis Island Group.||Overlies transitionally, and is faulted against, Wandilla Formation. Is intruded by Miriam Vale Granodiorite.|Fine-grained, poorly sorted, thick quartzose sandstone beds, locally metamorphosed to quartz-muscovite-biotite schists and gneiss; alternating with grey to black, very thin-bedded to laminated mudstone; rare beds of chert or fine felsic tuff.|
16848|Shoalwater Formation|68319|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Wandilla Province.||||Facies variant of Gaythorn Metamorphics.|Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.|
16848|Shoalwater Formation|68421|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province.||||Conformably underlain by the Wandilla Formation.|Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.|
16848|Shoalwater Formation|68679|5|Briefly described|p317-319, p324, p336, p338, p420, p469|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province, New England Orogen. Forms a chain of islands in Keppel Bay, a thin strip along eastern Curtis island to Facing Island, and reaches the mainland S of Gladstone. Estimated thickness of 10,000m is a gross exaggeration due to fault repetition. Chert or tuff beds crop out as strike ridges. Deep marine deposits. Deformation described. Contains unidentifiable plant fragments in black shales.||Curtis Island Group.||Conformably (transitionally) overlies Wandilla Formation. Possible correlative of Bjelke-Petersen beds. Is intruded by Chowey and Mingo Granites.|Quartzose sandstone beds (to 3m thick), fine- to medium-grained, poorly sorted, locally graded, locally metamorphosed to schist and gneiss; alternating with very thin-bedded to laminated mudstone beds; rare beds of chert or fine felsic tuff.|
16848|Shoalwater Formation|69952|6|Mentioned|p72|||New England Orogen. Forms hilly country.||||||
16848|Shoalwater Formation|73197|6|Mentioned|p468|||New England Orogen, northern. Coastal Subprovince. Deposited in outboard environment, contains range of zircon ages that were not sourced primarily from the Currabubula-Connors Arc, suggested to be from streams draining the continental interior.|||||Quartz-rich turbidites.|
16848|Shoalwater Formation|73201|6|Mentioned|p619|||New England Orogen. Outboard of a subduction complex.|||||Quartzose sandstones.|
16848|Shoalwater Formation|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, accretionary complex.|||||Includes quartz-rich, medium-grained sandstone.|
16848|Shoalwater Formation|73450|6|Mentioned|p21|Paleozoic|Paleozoic|||||Intruded by Molangul Granite.||
16860|Showgrounds Sandstone|13516|5|Briefly described|p138, p162-163, p166|Middle Triassic|Middle Triassic|From Bowen Basin. Shown in text as Showgrounds Sandstone, but in Figs p159, p169 as Showgrounds Sandstone Member. P163 suggests there are facies-relationship grounds for considering Showgrounds Sandstone to be a Member of Moolayember Formation rather than a Fm of Clematis Group.||Of Clematis Group||Diachronous contact with overlying Moolayember Formation||
16860|Showgrounds Sandstone|22857|6|Mentioned|p295, p315 Fig. 22.8|||Mentioned only in terms of equivalents of this unit.||||||
16860|Showgrounds Sandstone|22865|4|Described|p295,Fig22.8p315|Middle Triassic|Early Triassic|||||||
16860|Showgrounds Sandstone|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
16860|Showgrounds Sandstone|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
16860|Showgrounds Sandstone|23359|6|Mentioned|76|||||||||
16860|Showgrounds Sandstone|24069|5|Briefly described|p284|Middle Triassic|Middle Triassic|Geological Province: Surat Basin.||||||
16860|Showgrounds Sandstone|24077|5|Briefly described|p411 Tb.3|Middle Triassic|Early Triassic|Of the Mimosa Group.  White coarse quartzose sandstone.  Max. thickness: 13m.  Geological Province: Bowen Basin.||||||
16860|Showgrounds Sandstone|24159|5|Briefly described|p148, Fig. 2|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin. Overlying Unit: Snake Creek Mudstone Member. Underlying Unit: unconformably with Kianga Formation.||||||
16860|Showgrounds Sandstone|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Middle Triassic|||||||
16860|Showgrounds Sandstone|29385|6|Mentioned|p82|||||||||
16860|Showgrounds Sandstone|29387|6|Mentioned|p29|||||||||
16860|Showgrounds Sandstone|29389|6|Mentioned|p17|||Early Triassic.||||||
16860|Showgrounds Sandstone|29390|6|Mentioned|p54|||Triassic resevoir for Roma.||||||
16860|Showgrounds Sandstone|29391|6|Mentioned|Table 4|||Appears on P19.||||||
16860|Showgrounds Sandstone|29393|6|Mentioned|Table 2|||Triassic.||||||
16860|Showgrounds Sandstone|29721|6|Mentioned|Table 65|||||||||
16860|Showgrounds Sandstone|30696|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|31115|6|Mentioned|p34|||||||||
16860|Showgrounds Sandstone|31369|4|Described|p30|||||||||
16860|Showgrounds Sandstone|33059|4|Described|Table 1|||M.Trias.||||||
16860|Showgrounds Sandstone|33530|5|Briefly described|Table 1|||Middle Triassic||||||
16860|Showgrounds Sandstone|34212|6|Mentioned|p1|||Triassic. See also PP2,3,4 etc.||||||
16860|Showgrounds Sandstone|36111|6|Mentioned|p34|||||||||
16860|Showgrounds Sandstone|36613|6|Mentioned|Table 4|||||||||
16860|Showgrounds Sandstone|36643|6|Mentioned|p61|||||||||
16860|Showgrounds Sandstone|36914|6|Mentioned|p85|||||||||
16860|Showgrounds Sandstone|37288|6|Mentioned|p41|||||||||
16860|Showgrounds Sandstone|39445|5|Briefly described|Table 9|||||||||
16860|Showgrounds Sandstone|39491|4|Described|p18|||||||||
16860|Showgrounds Sandstone|39494|6|Mentioned|p137|||||||||
16860|Showgrounds Sandstone|39815|6|Mentioned|p445|||||||||
16860|Showgrounds Sandstone|40030|6|Mentioned|p135|||||||||
16860|Showgrounds Sandstone|40249|6|Mentioned|p41|||||||||
16860|Showgrounds Sandstone|40544|6|Mentioned|p161|||||||||
16860|Showgrounds Sandstone|40767|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|41188|6|Mentioned|p231|||||||||
16860|Showgrounds Sandstone|41210|6|Mentioned|p163|||||||||
16860|Showgrounds Sandstone|41247|6|Mentioned|p117|||||||||
16860|Showgrounds Sandstone|41712|6|Mentioned|p275|||See also Fig.5||||||
16860|Showgrounds Sandstone|41725|6|Mentioned|p400|||See also P403||||||
16860|Showgrounds Sandstone|42250|6|Mentioned|p28|||||||||
16860|Showgrounds Sandstone|42618|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|42634|5|Briefly described|Table 2 P10|||||||||
16860|Showgrounds Sandstone|42911|6|Mentioned|p20|||||||||
16860|Showgrounds Sandstone|43000|6|Mentioned|p108|||||||||
16860|Showgrounds Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
16860|Showgrounds Sandstone|43185|6|Mentioned|6||Triassic|||||||
16860|Showgrounds Sandstone|43711|6|Mentioned|p17|||||||||
16860|Showgrounds Sandstone|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
16860|Showgrounds Sandstone|43883|14|Not recorded|p18 Fig.4-3|||Misspelling of 'Showground Ss'?||||||
16860|Showgrounds Sandstone|43960|14|Not recorded|p9,12||Triassic|||||||
16860|Showgrounds Sandstone|44116|14|Not recorded|p24,28|||||||||
16860|Showgrounds Sandstone|44422|14|Not recorded|p150,155|Late Triassic|Middle Triassic|=Clematis Sandstone.||||||
16860|Showgrounds Sandstone|44787|14|Not recorded|Tb.p121-125,127-128||Late Triassic|Equivalent to upper part of Clematis Sandstone.||||||
16860|Showgrounds Sandstone|45110|6|Mentioned|p52|||||||||
16860|Showgrounds Sandstone|61313|6|Mentioned|p105|||Equivalent to Digby Formation and the shales of Napperby Formation. Geological Province: Surat Basin||||||
16860|Showgrounds Sandstone|62357|5|Briefly described|p524 Fig. 7, p535|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16860|Showgrounds Sandstone|64048|5|Briefly described|p67|Middle Triassic|Middle Triassic|Commercial gas production in its fluvial quartzose sandstones.||||||07-FEB-11
16860|Showgrounds Sandstone|64197|6|Mentioned|p630 Fig.7|Triassic|Triassic|||||Underlies the Moolayember Formation. Overlies the Rewan Group.||
16860|Showgrounds Sandstone|64856|4|Described|p42, p69-76, p78|Anisian|Anisian|Named but not defined by Derrington and Mott (1955). Bowen Basin. Medium to very coarse grained sandstone equivalent to upper part of the Clematis Group (Expedition Sandstone). Unconformable on the Rewan Group on the Roma Shelf and southwest Taroom Trough. Is overlain by Snake Creek Mudstone Member (Moolayember Formation). Contains palynofloras APT31 age (237.5-240 Ma).|| ||||29-NOV-17
16860|Showgrounds Sandstone|64857|5|Briefly described|p126-128, p113 Fig. 3|Triassic|Triassic|Bowen Basin. Mainly medium to coarse grained quartzose sandstone and conglomerate. Correlative of the Expedition Sandstone. Appears to be a member of the Clematis Group. Conformably underlies Snake Creek Mudstone Member.||||||15-JUL-13
16860|Showgrounds Sandstone|64858|6|Mentioned|p180 Fig.2|Middle Triassic|Middle Triassic|||||||30-NOV-09
16860|Showgrounds Sandstone|64859|6|Mentioned|p194|Middle Triassic|Middle Triassic|Hydrocarbon reservoir, Bowen Basin.||||||
16860|Showgrounds Sandstone|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Middle Triassic|Unit in the Bowen Basin. Top unit in the Clematis Group of the Taroom Trough.||||Overlain by Moolayember Formation.||22-MAR-12
16860|Showgrounds Sandstone|65113|5|Briefly described|Fig 4 p340|Early Triassic|Early Triassic|Sst, in text. Underlies the Moolayember Formation.||||||
16860|Showgrounds Sandstone|65114|5|Briefly described|p385 Fig.3|Middle Triassic||||||||
16860|Showgrounds Sandstone|65115|5|Briefly described|p425, 426, Fig 2 p403|Triassic|Triassic|Of Clematis Group, Taroom Trough? Underlies the Moolayember Formation in the Taroom Trough, Bowen Basin. Part of Supersequence I.||||||
16860|Showgrounds Sandstone|65116|5|Briefly described|p450, 451, Fig 2 p436|Middle Triassic|Early Triassic|Of Clematis Group. Underlies the Moolayember Formation in the Bowen Basin.||||||
16860|Showgrounds Sandstone|65118|5|Briefly described|p493, Fig 2 p479|Triassic|Triassic|Of Clematis Group? Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Unconformably overlies the Rewan Group||||||06-MAR-12
16860|Showgrounds Sandstone|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
16860|Showgrounds Sandstone|67402|4|Described|p18 fig WSD2, p19 fig WSD3, WSD4|Anisian|Anisian|Bowen and Surat Basins. Proven hydrocarbon reservoir and potential carbon dioxide storage reservoir. Deposited in a fluvial-deltaic environment. See also p30, p43 tbl HPB1, p45-49, p52, p53, p55-p57, p59, p62, p144, p147 fig SRT5, p300.||||Conformably overlain by the Snake Creek Mudstone. Overlies the Rewan Group.|Quartzose sandstone and conglomerate with some interbedded siltstone and shale.|
16860|Showgrounds Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Clematis Group.||||
16860|Showgrounds Sandstone|68004|5|Briefly described|p87, p172, p173, p175.|Middle Triassic|Middle Triassic|Surat Basin. Hydrocarbon reservoir in Queensland; targeted for oil/gas exploration in New South Wales from the 1960s; only minor fluorescence and low level gas shows. Sealed by Moolayember Formation. Discussed in some detail.||||||
16860|Showgrounds Sandstone|68679|5|Briefly described|p377, p381, p383-384|Middle Triassic|Middle Triassic|Traves and Thralls (1960). Roma Shelf, Bowen Basin. <40m thick. Braided fluvial stream deposits. Produces oil, gas and condensate.||||Overlies the Rewan group. Is overlain by the Moolayember Formation. Equivalent to upper Clematis Group in Roma area. Laterally equivalent to Expedition Sandstone.|Medium-grained to very coarse-grained quartzose sandstone, minor granule to pebble conglomerate.|
16860|Showgrounds Sandstone|69582|6|Mentioned|p35|||Surat Basin.||||Overlain by the Moolayember Formation.||
16860|Showgrounds Sandstone|72297|5|Briefly described|p744-745|||Western side of the Taroom Trough, Bowen Basin. A significant regional hydrocarbon reservoir; channel sandstones. Traps are structural-stratigraphic formed by later deformation.||Clematis Group.||||
16860|Showgrounds Sandstone|73113|6|Mentioned|p46|||Bowen Basin. Written as equivalent to Clematis Group [now a constituent].||||||
16881|Silkstone Formation|29720|6|Mentioned|p79|||||||||
16881|Silkstone Formation|30086|5|Briefly described|p4|||||||||
16881|Silkstone Formation|30087|4|Described|p3|||See also p4. Unit of Booval Group.||||||17-SEP-08
16881|Silkstone Formation|31132|6|Mentioned|p150|||||||||
16881|Silkstone Formation|33368|6|Mentioned|p49|||Low grade oil shale reported.||||||
16881|Silkstone Formation|33381|4|Described|p121|||See also p123. Tertiary.||||||17-SEP-08
16881|Silkstone Formation|34070|6|Mentioned|p3|||Tertiary||||||
16881|Silkstone Formation|34287|6|Mentioned|p202|||||||||
16881|Silkstone Formation|34354|6|Mentioned|p3|||Tertiary. See P12.||||||
16881|Silkstone Formation|34505|6|Mentioned|p3|||Booval Group. See Fig.8||||||
16881|Silkstone Formation|36779|6|Mentioned|p8|||||||||
16881|Silkstone Formation|38074|5|Briefly described|Table 1|||||||||
16881|Silkstone Formation|38080|6|Mentioned|p54|||||||||
16881|Silkstone Formation|38441|6|Mentioned|Map legend|Eocene|Paleocene|Palaeocene - Eocene||||||
16881|Silkstone Formation|39445|5|Briefly described|Table 14|||||||||
16881|Silkstone Formation|40623|5|Briefly described|p31|||||||||
16881|Silkstone Formation|41906|3|Fully described|Table 4 P33|||||||||
16881|Silkstone Formation|42336|4|Described|p6|||||||||
16881|Silkstone Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
16881|Silkstone Formation|43995|14|Not recorded|Tb.p10||Tertiary|||||||
16881|Silkstone Formation|44510|14|Not recorded|Fig.36|||||||||
16881|Silkstone Formation|44581|2|Defined|p346-348||Oligocene|Conformably overlies Redbank Plains Formation.||||||
16881|Silkstone Formation|44603|14|Not recorded|p129|||||||||
16881|Silkstone Formation|44687|6|Mentioned|p221,226|||Equivalent of Corinda Formation.||||||21-MAR-13
16881|Silkstone Formation|44704|14|Not recorded|p1,4,6,10|||||||||
16881|Silkstone Formation|44734|14|Not recorded|p6,13-15||Oligocene|Alternations of limestone and basalt; Pine Mountain area.||||||
16881|Silkstone Formation|44771|14|Not recorded|p3||Tertiary|||||||
16881|Silkstone Formation|44775|14|Not recorded|Map 2||Tertiary|||||||
16881|Silkstone Formation|44776|14|Not recorded|p4,fig.3|Oligocene|Eocene|Unit of Booval Group.||||||
16881|Silkstone Formation|44783|14|Not recorded|p2,11-13|||||||||
16881|Silkstone Formation|44784|14|Not recorded|p12||Oligocene|||||||
16881|Silkstone Formation|44786|14|Not recorded|p193-202||Cenozoic|Early Cainozoic (?Oligocene)||||||19-NOV-08
16881|Silkstone Formation|44810|14|Not recorded|p167 (Tb.)||Oligocene|||||||
16881|Silkstone Formation|44813|14|Not recorded|p80,82,84,|Oligocene|Eocene|||||||
16881|Silkstone Formation|45087|5|Briefly described|p154|||Chemical analyses||||||
16881|Silkstone Formation|61155|5|Briefly described|p19|Middle Eocene|Early Eocene|Of the Booval Group. Overlies the Redbank Plains Formation; overlain by Beaudesert Beds and Petrie Formation. Age: 55-51Ma. Thickness: ~278m. In the Brisbane region.||||||
16881|Silkstone Formation|68579|2|Defined|p221, 222|Oligocene|Eocene|After Silkstone Series of Bryan and Jones (1946). Type area NE corner of Queen's Park Ipswich. Max observed thickness 913 ft (basal 300ft is basalt). Gastropod fauna, possible fish. Age probably Oligocene.||||Conformably overlies Redbank Plains Formation.|Mudstones, clays and fissile shales; oil shales; dolomitic limestone sometimes completely replaced by chalcedonic silica; interbedded vesicular basalt flows; some pyroclastic material.|26-APR-13
16881|Silkstone Formation|69599|5|Briefly described|p586, p594-595|Eocene|Eocene|Booval Basin. 278m thick. Capped by laterite and silcrete. Middle Eocene.||Booval Group.||Conformably overlies Redbank Plains Formation. Is correlated with Corinda Formation.|Basal basalt flows (~110m), with an overlying mud-dominated unit of claystone, shale and minor oil shale (total 90m), capped by an upper magnesian limestone with fossil freshwater gastropods (50m).|
16882|Siltstone Member|22954|6|Mentioned|Fig3p9|||||||||
16882|Siltstone Member|47058|5|Briefly described|p132|||part of Monastery Creek Formation. May have intended informal usage.||||||
16882|Siltstone Member|60264|5|Briefly described|p575|Middle Cambrian|Middle Cambrian|Lower section of the Monastery Creek Formation.  White fissile siltstone, chert, and minor pelletal phosphorite.  Max. thickness: 60m.  Geological Province: Burke River Outlier.||||||02-AUG-04
16892|Silver Spur beds|37509|6|Mentioned|p504|||||||||
16892|Silver Spur beds|39252|6|Mentioned|p22|||||||||
16892|Silver Spur beds|42559|6|Mentioned|p24|||||||||
16892|Silver Spur beds|43008|5|Briefly described|map legend|||||||||
16892|Silver Spur beds|43017|5|Briefly described|Fig.2,p374|||||||||
16892|Silver Spur beds|44093|5|Briefly described|p212 App. 1|Early Permian|Early Permian|Clastic sediments. Unmetamorphosed to low grade metamorphism. Geological Province: New England Fold Belt.||||||
16892|Silver Spur beds|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Medium to thick bedded volcaniclastic arenite, mudstone, conglomerate and minor limestone.||||||11-DEC-07
16892|Silver Spur beds|63748|4|Described|p16-17|Early Permian|Early Permian|Dominated by steeply dipping to vertical sequences of rhythmically interbedded mudstone and arenite. Detailed lithology provided. Beds host minerlisation. Within the Silver Spur Subprovince. Also mentioned: p68.||||||07-FEB-11
16892|Silver Spur beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Bondonga, Pikedale and Terrica beds, are all mapped under the symbol, Par.||||||
16892|Silver Spur beds|68679|5|Briefly described|p451, p455|Permian|Permian|Silver Spur Subprovince, Woolomin Province. 7km E of Texas. Beds are steeply-dipping to vertical. Associated with Cu, Cu-Pb, Ag mineralisation. Has early Permian marine macrofossils.|||||Rhythmically interbedded mudstone and sandstone; fine-grained beds commonly show low-grade metamorphism and pencil cleavage; coarser sandy horizons commonly show internal lamination and are preferentially silicified. Local limestone, basalt.|
16892|Silver Spur beds|68901|5|Briefly described|p8 Fig. iii|Permian|Permian|||||||27-SEP-18
16892|Silver Spur beds|70373|4|Described|p789-p792, p795, p797 Tb 1, p798-p804|Early Permian|Early Permian|Lower Permian (Cisuralian) age derived from marine macrofossils which show similarities to fossils in Alum Rock beds. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. Contain clasts of chert, sandstone, volcanic rocks thought to be derived from Texas beds.|281.8+/-5.2 Ma (LA-ICP-MS on zircons)|||Unconformably overlie and/or faulted against Texas beds. Correlated with Bondonga, Pikedale, Terrica and Alum Rock beds.|Sandstone, pebbly sandstone, conglomerate, diamictite and mudstone with clasts of chert, sandstone and volcanics.|
16903|Silverwood Group|22601|6|Mentioned|405|Devonian|Devonian|||||||
16903|Silverwood Group|23423|5|Briefly described|p267|||||||||
16903|Silverwood Group|23811|5|Briefly described|Map Legend|Emsian|Pridoli|Tuffaceous mudstone, fine-grained, intermediate to basic igneous rocks with minor lithic wacke, foliated metaclaystone and metasiltstone, conglomerate, limestone breccia, chert and jasper.||||||20-DEC-04
16903|Silverwood Group|23812|4|Described|p9|Devonian|Silurian|Same as Willowie Creek beds of Fergusson, (1984), which are included in the group.||||||
16903|Silverwood Group|24612|5|Briefly described|p12|Devonian|Devonian|Contains Carlinastraea fauna.||||||06-APR-05
16903|Silverwood Group|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
16903|Silverwood Group|31694|6|Mentioned|p346|||||||||
16903|Silverwood Group|31802|6|Mentioned|p137|||||||||
16903|Silverwood Group|31999|4|Described|p150|||Fig. 2||||||
16903|Silverwood Group|32359|5|Briefly described|p736|||||||||
16903|Silverwood Group|32360|6|Mentioned|p748|||||||||
16903|Silverwood Group|32491|5|Briefly described|p7|Early Devonian|Silurian|||||||
16903|Silverwood Group|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian to Lower Devonian.||||||14-APR-08
16903|Silverwood Group|32494|6|Mentioned|p84|||||||||
16903|Silverwood Group|32880|6|Mentioned|p2|||Dev.||||||
16903|Silverwood Group|33091|6|Mentioned|p6|||Refers Olgers &  Flood (1970)||||||
16903|Silverwood Group|33146|5|Briefly described|p2|||See also P3. ?Sil.-L.Dev.||||||
16903|Silverwood Group|33436|6|Mentioned|p243|||Devonian. Refers Lucas (1959).||||||
16903|Silverwood Group|33437|6|Mentioned|p61|||L.Dev. Conodonts also on PP62-68||||||
16903|Silverwood Group|33476|6|Mentioned|p50|||||||||
16903|Silverwood Group|33561|6|Mentioned|p102|||||||||
16903|Silverwood Group|33703|6|Mentioned|p207|||||||||
16903|Silverwood Group|34479|6|Mentioned|p309|||See also P312. Devonian||||||
16903|Silverwood Group|35311|6|Mentioned|p207|||||||||
16903|Silverwood Group|35652|4|Described|p5|||||||||
16903|Silverwood Group|36045|6|Mentioned|p325|||||||||
16903|Silverwood Group|36716|6|Mentioned|p141|||||||||
16903|Silverwood Group|36961|6|Mentioned|p205|||||||||
16903|Silverwood Group|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
16903|Silverwood Group|37509|6|Mentioned|p504|||||||||
16903|Silverwood Group|38806|6|Mentioned|p71|||||||||
16903|Silverwood Group|39445|6|Mentioned|p67|||Early Devonian with Late Ord. limestone blocks. See also Fig.8 & Table 5||||||
16903|Silverwood Group|39673|6|Mentioned|Fig. 3a|||||||||
16903|Silverwood Group|40245|6|Mentioned|p198|||||||||
16903|Silverwood Group|40246|6|Mentioned|p164|||||||||
16903|Silverwood Group|40435|6|Mentioned|p49|||||||||
16903|Silverwood Group|40514|6|Mentioned|p4|||||||||
16903|Silverwood Group|40960|6|Mentioned|p216|||||||||
16903|Silverwood Group|42031|5|Briefly described|Fig.8 P766|||||||||
16903|Silverwood Group|42140|6|Mentioned|p560|||||||||
16903|Silverwood Group|42297|6|Mentioned|Fig. 5 P5|Devonian||||||||
16903|Silverwood Group|42559|5|Briefly described|p7|||||||||
16903|Silverwood Group|42997|6|Mentioned|p38|||||||||
16903|Silverwood Group|43008|5|Briefly described|map legend|||||||||
16903|Silverwood Group|43083|6|Mentioned|p39|||Includes Rosenthal Creek Formation.  In the Warwick-Stanthorpe area.||||||17-JUN-09
16903|Silverwood Group|43461|14|Not recorded|Table p618|Middle Devonian|Early Devonian|L.-L.M.Dev||||||
16903|Silverwood Group|43745|6|Mentioned|Fig.4,p13|||||||||
16903|Silverwood Group|44070|14|Not recorded|p141|||||||||
16903|Silverwood Group|44091|14|Not recorded|p34|Middle Devonian|Early Devonian|||||||
16903|Silverwood Group|44093|5|Briefly described|p119|Early Devonian|Early Devonian|||||||
16903|Silverwood Group|44269|14|Not recorded|p14||Devonian|Lower or Middle Devonian.||||||
16903|Silverwood Group|44429|14|Not recorded|p228-229|||See also Lexicon.||||||
16903|Silverwood Group|44512|14|Not recorded|p15,16||Devonian|Ref. to Lucas 1960. See also Lexicon.||||||
16903|Silverwood Group|44563|14|Not recorded|p142-143|||See also Lexicon.||||||
16903|Silverwood Group|44783|14|Not recorded|p2,43-45|||||||||
16903|Silverwood Group|44786|14|Not recorded|p193-202|Middle Devonian|Early Devonian|||||||
16903|Silverwood Group|48940|6|Mentioned|p12|||Refers Richards & Bryan (1923)||||||
16903|Silverwood Group|60937|5|Briefly described|p424 Fig. 2|||||||||
16903|Silverwood Group|61392|3|Fully described|p163-165, p166|Early Carboniferous|Middle Cambrian|Also referred to as the Keinjan Terrane. Incl: Risdon Stud Fm, Connolly Volcs, Bald Hill Fm, Ormoral Volcs and Bromley Hills Fm. Comprises various lithologies. Effectively the same sequence as Willowie Creek beds.||||||07-FEB-11
16903|Silverwood Group|63731|5|Briefly described|Map legend|Devonian|Silurian|Includes Risodon Stud and Bald Hill Formations, Connolly, Ormoral and Bromley Hills Volcanics.||||||
16903|Silverwood Group|63732|5|Briefly described|Map legend|Devonian|Silurian|Mafic-dominated volcaniclastic deposits, lavas and subvolcanic metabasite sills; massive to thin-bedded volcaniclastic and epiclastic sediments+some chert; local conglom.+debris-flow deposits. Fine-gr.metadolerite and metabasalt.||||||
16903|Silverwood Group|63748|4|Described|p6, p7 Fig. 3|Paleozoic|Paleozoic|Formerly incl: Risdon Stud Fm, Connolly Volcs + Rosenthal Fm. Revised by Van Noord (1999b) to retain Risdon Stud Fm + Connolly Volcs but remainder now divided into Bald Hill Fm overlain by Omoral Volcanics + Bromley Hills Fm. Geol.prov:Silverwood Province||||||07-FEB-11
16903|Silverwood Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Silverwood Province.||||||
16903|Silverwood Group|68679|5|Briefly described|p321, p444-447, p452-453, p455-456|Devonian|Silurian|Silverwood Province, northern New England Orogen. An oceanic arc sequence. Exposed as a roughly triangular area ~100 km2 between Warwick and the NSW border. Previously included the Rosenthal Creek Formation (Olgers et al., 1974), but this unit was divided by Van Noord (1999) into the three upper units. RELATED UNITS (continued): Is intruded by Herries Granite.|||Risdon Stud Formation, Connolly Volcanics, Bald Hill Formation, Ormoral Volcanics and Bromley Hills Formation.|Is faulted against the Eurydesma, Condamine, Wallaby, Eight Mile Creek, Rhyolite Range, beds (or is overlain unconformably by these last two). Equivalent to Willowie Creek beds in NSW. See COMMENTS.|Marine volcaniclastic, clastic and volcanic rocks.|
16903|Silverwood Group|68822|6|Mentioned|p336|||||||||
16903|Silverwood Group|68901|5|Briefly described|p8 Fig. iii|Devonian|Silurian|Silverwood Province.||||||27-SEP-18
16903|Silverwood Group|69639|6|Mentioned|p151|||||||Intruded by the Maryland Granite.|Sediments.|
16903|Silverwood Group|71628|5|Briefly described|p9:11-13, 15, 19, 23, 25, 27, 35; p11-26|Devonian|Silurian|See also p15: 33, 57, 69; p16-4; p18-13; p19: 59, 67, 97, 128, 147-148, 163. Apparently equivalent to Willowie Creek beds [?Beds] of Fergusson (1984). RELATED UNITS (continued): Is also intruded by Cullendore Syenogranite and all units of Dumbudgery Creek Complex. Is faulted against The Ridge Monzogranite.|||Connolly Volcanics; Bald Hill, Risdon Stud Formations; Willowie Creek beds.|Is intruded by Towgon Grange and Kaloe Tonalites, Rocky River and Moonta Gully Monzogranites, Mount Lindesay Monzogranite (Stanthorpe Complex). See COMMENTS for more.|Mafic to intermediate tuffs, flows and shallow intrusives with intercalated conglomerates, sandstones, tuffaceous argillites and altered limestones.|
16903|Silverwood Group|73143|6|Mentioned|p14|Early Devonian|Ludlow|Contains Heliolites tabulate coral (Jones and Hill, 1940).||||||
16903|Silverwood Group|73197|5|Briefly described|p460 Fig.1, p463, p464 Fig.3|Late Devonian|Silurian|New England Orogen, southern. Fragments of the obducted Silurian-late Devonian Calliope-Gamilaroi Oceanic Arc. Lithologies described are in relation to various outcrops of the Silverwood Group, Calliope Province and Gamilaroi Terrane.|||||Mix of rock types including felsic volcanic rocks and tuff, volcaniclastic sandstone and conglomerate, limestone, mudstone and, in the upper sequences, pillow basalt and dolerite.|
16909|Sim Jue Creek Granodiorite|36440|6|Mentioned|Map legend|Early Triassic|Late Permian|Early Triassic to Late Permian||||||
16909|Sim Jue Creek Granodiorite|39079|6|Mentioned|p8|||||||||
16909|Sim Jue Creek Granodiorite|42525|5|Briefly described|Map legend|Triassic|Permian|||||||
16949|Sirius Mudstone Member|13516|5|Briefly described|p145 fig 3,  p146 fig 4, p150|Early Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP321||Cattle Creek Formation||||
16949|Sirius Mudstone Member|29721|6|Mentioned|Table 65|||||||||
16949|Sirius Mudstone Member|30449|6|Mentioned|p2|||Brachiopods. See also P14,16||||||
16949|Sirius Mudstone Member|30826|6|Mentioned|Fig.1|||||||||
16949|Sirius Mudstone Member|31120|4|Described|p150|||||||||
16949|Sirius Mudstone Member|31305|6|Mentioned|p569|||||||||
16949|Sirius Mudstone Member|32139|6|Mentioned|p582|||See Table||||||
16949|Sirius Mudstone Member|32577|4|Described|p23|||See also P24,32,33,44. L.Perm.||||||
16949|Sirius Mudstone Member|32840|6|Mentioned|p29|||||||||
16949|Sirius Mudstone Member|32943|6|Mentioned|p106|||See also Fig.2||||||
16949|Sirius Mudstone Member|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships||||||
16949|Sirius Mudstone Member|36243|6|Mentioned|Table 3A|||||||||
16949|Sirius Mudstone Member|36739|6|Mentioned|p19|||||||||
16949|Sirius Mudstone Member|37705|6|Mentioned|Fig.2|||||||||
16949|Sirius Mudstone Member|37726|6|Mentioned|Fig.2|||||||||
16949|Sirius Mudstone Member|39263|6|Mentioned|Fig.2|||||||||
16949|Sirius Mudstone Member|39273|6|Mentioned|p305|||||||||
16949|Sirius Mudstone Member|39423|6|Mentioned|p53|||||||||
16949|Sirius Mudstone Member|39943|6|Mentioned|Table 5A|||||||||
16949|Sirius Mudstone Member|41605|6|Mentioned|Fig.2|||||||||
16949|Sirius Mudstone Member|42578|6|Mentioned|Table 1 P124-125|||||||||
16949|Sirius Mudstone Member|43050|5|Briefly described|p6|||Of Cattle Creek Formation.||||||17-MAR-09
16949|Sirius Mudstone Member|43737|6|Mentioned|p5||Kungurian|||||||
16949|Sirius Mudstone Member|44172|14|Not recorded|Tb.1,p1325||Artinskian|Springsure area.||||||
16949|Sirius Mudstone Member|44173|14|Not recorded|p109-110||Early Permian|Formerly Sirius Formation. Member of Cattle Creek Formation.||||||
16949|Sirius Mudstone Member|45071|3|Fully described|Table 6|||||||||
16949|Sirius Mudstone Member|46849|6|Mentioned|Fig. 7|||||||||
16949|Sirius Mudstone Member|60286|4|Described|p274|Early Permian|Early Permian|Top member of Cattle Creek Formation. Overlain by Lower Aldebaran Sandstone. Prodelta deposits. Geological Province: Bowen Basin.||||||09-FEB-05
16949|Sirius Mudstone Member|61612|6|Mentioned|p270, p276, p270 Fig. 1|Early Permian|Early Permian|Of Cattle Creek Formation. Geological Province: Denison Trough. QLD.||||||17-MAR-09
16949|Sirius Mudstone Member|68576|5|Briefly described|Q_4: p3, p5, p7-8, p19, p24|Cisuralian|Cisuralian|Bowen Basin. Abbreviated to Sirius Mudstone on p5 and p24. Records a major marine transgression.||Cattle Creek Formation.||Overlies Staitrcase Sandstone Member and Reids Dome beds. Is overlain by Aldebaran Sandstone.|Laminated and thinly-bedded, light to dark grey siltstone, shale, mudstone and fine to very fine labile sandstone. Some plant fragments and pyrite are present. Fossil shells and calcareous veins occur.|
16949|Sirius Mudstone Member|68731|6|Mentioned|p201 Fig 3.110, p206|Cisuralian|Cisuralian|Bowen Basin. Age constrained by the Cattle Creek Formation.||Of the Cattle Creek Formation.||||
16949|Sirius Mudstone Member|71265|5|Briefly described|p589|Guadalupian|Cisuralian|Bowen Basin.||Cattle Creek Formation.||Overlies Reids Dome beds. Is overlain by Aldebaran Sandstone.||
16949|Sirius Mudstone Member|71701|5|Briefly described|p155|Kungurian|Kungurian|Denison Trough, Bowen Basin.||Cattle Creek Formation||||
16949|Sirius Mudstone Member|72088|5|Briefly described|p8, p91|Roadian|Kungurian|Eastern Galilee Basin and Denison Trough, Bowen Basin.||||Unconformably overlies the Reids Dome beds and the Cattle Creek Formation. Overlain by the Aldebaran Sandstone.||
16949|Sirius Mudstone Member|73472|6|Mentioned|p115|Kungurian|Kungurian|||Cattle Creek Formation||Underlain by Reids Dome beds. Overlain by Aldebaran Sandstone.||
16991|Slaughter Yard Creek Volcanics|23423|4|Described|p304 Table 7.3||Early Permian|Intruded by Watsonville Granite. Intrudes Jumna and Saint Patrick Hill Granite and Kalunga Granodiorite. Age: ~275 +/- 3 Ma. Also see p237.  Kennedy Igneous Province. Maximum thickness >100 m.||||||
16991|Slaughter Yard Creek Volcanics|23506|5|Briefly described|Map Legend||Early Permian|Age: ~275+/-3Ma Rb-Sr.||||||
16991|Slaughter Yard Creek Volcanics|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V81. I-Type.||||||
16991|Slaughter Yard Creek Volcanics|23616|5|Briefly described|Table 3 p44||Early Permian|Unit intruded by Watsonville Granite, and is unconformable on and/or intrudes the Jumna and St Patrick Hill Granites and Kalunga Granodiorite. Originally mapped as Glen Gordon Volcs (Best 1962) & delineated by Blake (1972). Of Koolmoon Volcanic Group||||||
16991|Slaughter Yard Creek Volcanics|33205|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16991|Slaughter Yard Creek Volcanics|37613|6|Mentioned|p252|||See also Fig.1.||||||
16991|Slaughter Yard Creek Volcanics|39445|6|Mentioned|p90|||Previuosly Glen Gordon Volc. on map||||||
16991|Slaughter Yard Creek Volcanics|43060|5|Briefly described|p73|||||||||
16991|Slaughter Yard Creek Volcanics|43259|4|Described|Appendix 1,p8 &p48||Permian|||||||
16991|Slaughter Yard Creek Volcanics|45065|4|Described|Table 4|||||||||
16991|Slaughter Yard Creek Volcanics|45113|3|Fully described|p26|||Emphasis on petrography.||||||
16991|Slaughter Yard Creek Volcanics|46845|6|Mentioned|Table 1|||||||||
16991|Slaughter Yard Creek Volcanics|48976|4|Described|p65|||Isotopic data Table 17||||||
16991|Slaughter Yard Creek Volcanics|60425|4|Described|p41, p44 Tb.3, p52|Early Permian|Early Permian|Unconformable on/or intrudes Jumna and Herberton Hill Granites+Kalunga Granodiorite. Age:~275+/-3Ma (RB-Sr).Thickness:>100m.Slightly porphyritic rhyolitic lava, highly porph.microgranite + intrusive rhyolite; minor volc.conglom/breccia. A-type affinities||||||07-FEB-11
17026|Snake Creek Mudstone Member|13516|5|Briefly described|p159, p162-163, p169, p138|Middle Triassic|Middle Triassic|From Bowen Basin||Of Moolayember Formation||Diachronous boundaries with rest of Moolayember Formation and underlying Showgrounds Sandstone.||
17026|Snake Creek Mudstone Member|23740|5|Briefly described|p1221|||Parent: Moolayenber Formation.  Geological Province: Bowen Basin||||||
17026|Snake Creek Mudstone Member|24159|5|Briefly described|p148 Fig.2, p149|Middle Triassic|Middle Triassic|Overlies the Showgrounds Sandstone. Geological Province: Bowen Basin.||||||
17026|Snake Creek Mudstone Member|29385|6|Mentioned|p82|||||||||
17026|Snake Creek Mudstone Member|29721|6|Mentioned|p70|||||||||
17026|Snake Creek Mudstone Member|31115|6|Mentioned|p35|||||||||
17026|Snake Creek Mudstone Member|31116|4|Described|p20|||||||||
17026|Snake Creek Mudstone Member|31369|2|Defined|p88|Middle Triassic|Middle Triassic|See also p33.||||||
17026|Snake Creek Mudstone Member|35295|6|Mentioned|p601|||||||||
17026|Snake Creek Mudstone Member|39491|6|Mentioned|p23|||||||||
17026|Snake Creek Mudstone Member|39494|6|Mentioned|Fig.5|||||||||
17026|Snake Creek Mudstone Member|40030|6|Mentioned|Fig.5|||||||||
17026|Snake Creek Mudstone Member|40120|6|Mentioned|p424|||||||||
17026|Snake Creek Mudstone Member|40249|6|Mentioned|p38|||||||||
17026|Snake Creek Mudstone Member|40544|6|Mentioned|p161|||||||||
17026|Snake Creek Mudstone Member|40767|6|Mentioned|p13|||||||||
17026|Snake Creek Mudstone Member|41188|6|Mentioned|p231|||||||||
17026|Snake Creek Mudstone Member|41247|6|Mentioned|Fig.7|||||||||
17026|Snake Creek Mudstone Member|42634|6|Mentioned|p11|||||||||
17026|Snake Creek Mudstone Member|61313|6|Mentioned|p105|||?Of the Showgrounds Sandstone? Equivalent to Digby Formation and the shales of Napperby Formation. Geological Province: Surat Basin.||||||
17026|Snake Creek Mudstone Member|61377|5|Briefly described|p151|Middle Triassic|Middle Triassic|A uniform dark grey-black shale. Conformably overlies Showgrounds Sandstone; conformably overlain by the Moolayember Formation. Provides a good regional seal for Showgrounds Sandstone reservoirs. Geological Province: Surat Basin.||||||15-JUL-13
17026|Snake Creek Mudstone Member|61612|6|Mentioned|p276, p277, p270 Fig. 1|Middle Triassic|Middle Triassic|Of Moolayember Formation. QLD. Lacustrine flooding event.||||||17-MAR-09
17026|Snake Creek Mudstone Member|64856|4|Described|p42, p70 Fig.17, p73-77, p102|Middle Triassic|Middle Triassic|Defined by Hogetoorn (1970). Predominantly dark grey to black mudstone with minor laminae and thin beds of very fine grained sandstone. Bottom unit of the Moolayember Formation, conformably overlies Clematis Group, Showgrounds Sandstone. Palynoflora age APT31-32 (235-240 Ma). 41m thick.|| ||||29-NOV-17
17026|Snake Creek Mudstone Member|64857|4|Described|p126-128, 129, 134, p113 Fig. 3|Triassic|Triassic|Bowen Basin. Member of the Moolayember Formation. Consists mainly of mudstone with minor very fine grained quartzose sandstone. Conformable on Showgrounds Sandstone. Genetically related to underlying Showgrounds Sandstone, rather than overlying Moolayember Formation.||||||
17026|Snake Creek Mudstone Member|64858|6|Mentioned|p180 Fig.2|Middle Triassic|Middle Triassic|Of Moolayember Formation?||||||16-MAR-12
17026|Snake Creek Mudstone Member|64859|5|Briefly described|p222-3, p225, 226, 193, 196, |Triassic|Triassic|Of Moolayember Formation.||||||
17026|Snake Creek Mudstone Member|65115|5|Briefly described|p426, 427|||of Moolayember Formation. Widespread lacustrine sediments.||||||
17026|Snake Creek Mudstone Member|65116|6|Mentioned|p451|Middle Triassic|Middle Triassic|||||||
17026|Snake Creek Mudstone Member|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||Unit in Moolayember Formation.||Overlies Showgrounds Sandstone.||
17026|Snake Creek Mudstone Member|68576|5|Briefly described|Q_4: p3, p21|Middle Triassic|Middle Triassic|Roma Shelf, Bowen Basin.||Moolayember Formation.||Overlies Clematis Group.|Mainly dark grey to black mudstone with minor laminae and thin beds of very fine-grained quartzose sandstone.|
17026|Snake Creek Mudstone Member|68679|5|Briefly described|p377, p383|Middle Triassic|Middle Triassic|Lake deposits.||Basal Moolayember Formation.|||Mudstone with lesser siltstone and sandstone.|
17026|Snake Creek Mudstone Member|72297|5|Briefly described|p744-745|||Bowen Basin. Lacustrine deposits. Potential hydrocarbon source rock. Forms a significant regional seal throughout the Basin.||Moolayember Formation.||||
17095|Somerset Dam Igneous Complex|30303|6|Mentioned|p323|||Rocks possibly related to this unit intrude Mount Byron Volcanics||||||
17095|Somerset Dam Igneous Complex|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
17095|Somerset Dam Igneous Complex|31811|6|Mentioned|Fig. 1|||||||||
17095|Somerset Dam Igneous Complex|35161|6|Mentioned|Fig.2|||||||||
17095|Somerset Dam Igneous Complex|36045|6|Mentioned|p335|||||||||
17095|Somerset Dam Igneous Complex|36440|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
17095|Somerset Dam Igneous Complex|36954|6|Mentioned|Table 4|||||||||
17095|Somerset Dam Igneous Complex|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
17095|Somerset Dam Igneous Complex|39079|6|Mentioned|p8|||||||||
17095|Somerset Dam Igneous Complex|39445|5|Briefly described|Table 12|||||||||
17095|Somerset Dam Igneous Complex|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
17095|Somerset Dam Igneous Complex|43008|5|Briefly described|map legend|||||||||
17095|Somerset Dam Igneous Complex|44783|14|Not recorded|p34|||||||||
17095|Somerset Dam Igneous Complex|65388|5|Briefly described|p323|Triassic|Permian|Southernmost of a chain of gabbroic intrusions extending from NW of Brisbane to SW of Rockhampton.||||||
17095|Somerset Dam Igneous Complex|68008|6|Mentioned|p435|||One of a chain of gabbro intrusions (listed) between Brisbane and Rockhampton.||||||
17095|Somerset Dam Igneous Complex|68679|5|Briefly described|p427-428|Late Triassic|Late Triassic|Esk area. A small, steep-sided unit. Other, mostly similar, ages given.|224.2 +/- 4.8 Ma (Ar-Ar: Walker, 1998).|||Intrudes Neara Volcanics.|A mafic phase including layered gabbro, and a late granophyric alkali feldspar granite.|
17116|South Kariboe Member|30451|5|Briefly described|p16|||See also Fig.2||||||
17116|South Kariboe Member|31999|5|Briefly described|p149|||||||||
17116|South Kariboe Member|32140|6|Mentioned|p9|||Dev. Dawes Range Fm.||||||
17116|South Kariboe Member|32865|6|Mentioned|p479|||Davies Range Fm. Fauna||||||
17116|South Kariboe Member|44379|2|Defined|p3-7,Tb.1,3,map||Late Devonian|Unit of Dawes Range Formation.||||||
17123|South Nicholson Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
17123|South Nicholson Group|22644|5|Briefly described|5,7|||Geological province: McArthur Basin.||||||04-DEC-06
17123|South Nicholson Group|22673|6|Mentioned|65,79|||Max thickness: 1000 m.||||||04-DEC-06
17123|South Nicholson Group|22680|4|Described|86|||||||||
17123|South Nicholson Group|23065|5|Briefly described|17|||Geological province: South Nicholson Basin.||||||04-DEC-06
17123|South Nicholson Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|23393|4|Described|p21, p17 Fig. 5|Mesoproterozoic|Mesoproterozoic|Geological Province: Lawn Hill Sub-province.||||||
17123|South Nicholson Group|23396|6|Mentioned|p425|||||||||
17123|South Nicholson Group|23404|5|Briefly described|p638 Fig.1|||||||||
17123|South Nicholson Group|23405|5|Briefly described|p586|||||||||
17123|South Nicholson Group|23406|5|Briefly described|p600 Fig. 2|||Age: <1500Ma.||||||16-JUN-09
17123|South Nicholson Group|23407|5|Briefly described|p633|||||||||
17123|South Nicholson Group|23409|5|Briefly described|p535 Fig.2|Mesoproterozoic|Mesoproterozoic|Of Lawn Hill Platform.||||||04-DEC-06
17123|South Nicholson Group|23519|5|Briefly described|p138|Mesoproterozoic|Mesoproterozoic|See also page 137 Fig 7||||||
17123|South Nicholson Group|23937|6|Mentioned|p22|||Correlated with the Roper Group - see p76 Appendix 1.||||||
17123|South Nicholson Group|23958|5|Briefly described|p1133|Mesoproterozoic|Mesoproterozoic|||||||
17123|South Nicholson Group|24047|6|Mentioned|p27|||Geological Province: South Nicholson Basin.||||||
17123|South Nicholson Group|24303|5|Briefly described|p59 Appendix|||Geological Province: Nicholson Basin. Correlative of Renner Group.||||||
17123|South Nicholson Group|24308|5|Briefly described|p995 Fig. 8|||||||||
17123|South Nicholson Group|24309|6|Mentioned|p1012 Fig. 1|||||||||
17123|South Nicholson Group|24419|5|Briefly described|p13 Fig.5|Mesoproterozoic|Mesoproterozoic|Geological Province: Murphy Province, Lawn Hill Subprovince (north), South Nicholson Basin.||||||
17123|South Nicholson Group|24432|6|Mentioned|p565 Fig.4|||||||||
17123|South Nicholson Group|24442|5|Briefly described|p22, p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1500-1450Ma. Geological Province: McArthur Basin.||||||
17123|South Nicholson Group|30344|6|Mentioned|p29|||Age: 1,510 +- 120m.y.||||||04-DEC-06
17123|South Nicholson Group|30508|6|Mentioned|p94|||Stratigraphy||||||
17123|South Nicholson Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|32659|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
17123|South Nicholson Group|32660|4|Described|Table 5|||||||||
17123|South Nicholson Group|32959|6|Mentioned|p31|||||||||
17123|South Nicholson Group|33214|6|Mentioned|Fig.1|||||||||
17123|South Nicholson Group|33900|6|Mentioned|p19|||||||||
17123|South Nicholson Group|34287|6|Mentioned|p41|||||||||
17123|South Nicholson Group|35114|6|Mentioned|p202|||||||||
17123|South Nicholson Group|35640|6|Mentioned|Map legend|Adelaidean|Adelaidean|Carpentarian||||||
17123|South Nicholson Group|35950|6|Mentioned|p311|||||||||
17123|South Nicholson Group|36003|6|Mentioned|p1029|||||||||
17123|South Nicholson Group|36012|3|Fully described|Table 4|||See also p16.||||||06-NOV-06
17123|South Nicholson Group|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||23-DEC-08
17123|South Nicholson Group|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
17123|South Nicholson Group|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17123|South Nicholson Group|37371|6|Mentioned|p368|||||||||
17123|South Nicholson Group|37459|6|Mentioned|p433|||See also p427.||||||04-DEC-06
17123|South Nicholson Group|37462|4|Described|Table4.VII|||||||||
17123|South Nicholson Group|37565|6|Mentioned|p3|||||||||
17123|South Nicholson Group|37568|6|Mentioned|p86|||||||||
17123|South Nicholson Group|37572|6|Mentioned|p155|||See also Fig.4||||||
17123|South Nicholson Group|38237|6|Mentioned|p125|||||||||
17123|South Nicholson Group|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17123|South Nicholson Group|38348|4|Described|p24|||||||||
17123|South Nicholson Group|38584|4|Described|p19|||||||||
17123|South Nicholson Group|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Includes the Mullera Formation and Constance Sandstone.||||||10-JAN-05
17123|South Nicholson Group|39445|5|Briefly described|p56|||See Table 3||||||
17123|South Nicholson Group|39497|6|Mentioned|p4|||||||||
17123|South Nicholson Group|39685|6|Mentioned|Fig.1|||||||||
17123|South Nicholson Group|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17123|South Nicholson Group|39925|6|Mentioned|p329|||||||||
17123|South Nicholson Group|40105|6|Mentioned|p315|||||||||
17123|South Nicholson Group|40840|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17123|South Nicholson Group|41721|6|Mentioned|p28|||Overlies the Doomadgee Formation and where this is missing it overlies Mount Les Siltstone or Walford Dolomite. Thickness: 300m+.  Geol. prov: South Nicholson Basin. Sandstone, siltstone and shale.||||||01-AUG-07
17123|South Nicholson Group|41722|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|41979|6|Mentioned|Fig.2 P512|||||||||
17123|South Nicholson Group|42385|5|Briefly described|Fig.4 P7|||||||||
17123|South Nicholson Group|42386|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17123|South Nicholson Group|42638|6|Mentioned|Map legend|||Appears on Regional Setting map. Age: Middle Proterozoic.|||||Quartz sandstone, micaceous siltstone and sandstone, shale.|07-NOV-11
17123|South Nicholson Group|42639|5|Briefly described|Fig.4 P7|||||||||
17123|South Nicholson Group|42775|6|Mentioned|Fig.13 P323|||||||||
17123|South Nicholson Group|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
17123|South Nicholson Group|43595|5|Briefly described|p440-1|||Shale Rb-Sr date at: 1480 Ma.||||||23-DEC-08
17123|South Nicholson Group|44287|14|Not recorded|p.12|||Equiv. of Roper Group. (E53-3).||||||
17123|South Nicholson Group|44305|14|Not recorded|p.14,15|||(E53-8). opp.p.6,18. Includes Mittiebah Sandstone, Mullera Formation, Constance Sandstone.||||||
17123|South Nicholson Group|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
17123|South Nicholson Group|44473|14|Not recorded|p.9-10,15,opp. p.7|||(E53-7). Represented in Wallhallow area by Mittiebah Sandstone.||||||
17123|South Nicholson Group|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
17123|South Nicholson Group|44482|14|Not recorded|p.7,8-10,opp.p.6,map|||(E53-12). See also p.14, for more details.||||||
17123|South Nicholson Group|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
17123|South Nicholson Group|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
17123|South Nicholson Group|45032|14|Not recorded|p9||Adelaidean|Tb.1, Pl.1.||||||
17123|South Nicholson Group|45052|4|Described|p69|||Adelaidean||||||
17123|South Nicholson Group|45166|4|Described|p33|||||||||
17123|South Nicholson Group|46804|6|Mentioned|p154|||||||||
17123|South Nicholson Group|46919|6|Mentioned|p221|||||||||
17123|South Nicholson Group|49001|6|Mentioned|p9|||||||||
17123|South Nicholson Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Roper Superbasin.||||||07-FEB-11
17123|South Nicholson Group|60675|6|Mentioned|Map legend|||||||||
17123|South Nicholson Group|61904|5|Briefly described|p132 Fig. 1|||||||||
17123|South Nicholson Group|62657|5|Briefly described|Map Legend|Calymmian|Calymmian|||||||
17123|South Nicholson Group|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|||||||
17123|South Nicholson Group|63113|6|Mentioned|p1212 Fig.1. |Mesoproterozoic|Mesoproterozoic|||||||
17123|South Nicholson Group|63114|6|Mentioned|p1270.|||Roper superbasin.||||||
17123|South Nicholson Group|64443|4|Described|iii, p3-5, p28, p40 |Calymmian|Calymmian|Basement to much of central Georgina Basin. Correlative of Renner Group and Roper Group; may unconformably underlie Barkly Group. Undivided South Nicholson Group contains lithologically undistinctive constituent units.|||Divided into Wild Cow and Accident Subgroups.|Is unconformably overlain by Wonarah Formation, Arthur Creek Formation, Thorntonia Limestone, Helen Springs Volcanics.||14-MAY-14
17123|South Nicholson Group|64575|6|Mentioned|p657|||||||||
17123|South Nicholson Group|64724|6|Mentioned|p45 Fig.5|Calymmian|Calymmian|South Nicholson Basin||||||
17123|South Nicholson Group|65336|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Accident Subgroup which includes Mittiebah Sandstone. Unconformably overlain by Kalkarindji Volcanic Group. Undifferentiated South Nicholson Group consists of quartz sandstone, mudstone, other sedimentary rocks.||||||
17123|South Nicholson Group|65337|4|Described|p6 Fig.3, p34, pp36-60.|Mesoproterozoic|Mesoproterozoic|Roper Superbasin. Occupies much of  MOUNT DRUMMOND outcrop area. To 6500 m thick, medial to proximal foreland basin deposits. Hosts several ironstone units, organic rich source rocks and potential reservoir formations.|c.1500-1400 Ma.||Includes Wild Cow and overlying Accident Subgroups.|Unconformably overlies Benmara and McNamara Groups. Is unconformably overlain by Bukalara Sandstone, Helen Springs Volcanics and Wonarah Formation.|Couplets of fine-grained shelf tempestites and shales, and coarse-grained fluvial and shallow-marine siliciclastic rocks.|
17123|South Nicholson Group|65340|5|Briefly described|p82.|||Unconformably overlies a group of diatremes of non-diamondiferous kimberlitic to lamproitic affinity at Coanjula.|1490 - 1430 Ma.|||||
17123|South Nicholson Group|65344|4|Described|p3, 5, 7,  9, 15-16, 21, Figs., Tables|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Underlies the Georgina Basin. Correlated with the Roper Group of the McArthur Basin. See well logs and thin section descriptions for detail.|||Includes the Mittiebah Sandstone.|Overlain by the Gum Ridge Formation, Thorntonia Limestone and Helen Springs Volcanics.|Mainly quartz sandstone.|
17123|South Nicholson Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Includes Mittiebah Sandstone.|Is unconformably overlain by Kiana Group.||13-APR-12
17123|South Nicholson Group|67149|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||||Is overlain by Helen Springs Volcanics.|Quartzose, lithic, micaceous and sublithic glauconitic sandstone, micaceous and ferruginous siltstone, shale, claystone; minor conglomerate, ironstone (cross-section only).|
17123|South Nicholson Group|67150|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Includes Accident Subgroup.|Is unconformably overlain by Helen Springs Volcanics and Gum Ridge Formation.|Quartzose, lithic, micaceous and sublithic glauconitic sandstone, micaceous and ferruginous siltstone, shale, claystone; minor conglomerate, ironstone (cross-section only).|
17123|South Nicholson Group|67323|5|Briefly described|GIS attrib tbl, p9, p11, p39, p107|Mesoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot. South Nicholson Basin. Age uncertain but likely to be in ~1500 - 1400 Ma range. Overlies Lawn Hill Platform rocks. CONSTITUENTS (continued): Middle Creek Sandstone Member, Mullera Formation, Pandanus Formation, Schultz Sandstone Member, Tidna Sandstone, Train Range Ironstone Member, Wallis Formation.|||Includes Bowthorn Siltstone Member, Burangoo Sandstone, Constance Sandstone, Elizabeth Sandstone Member, Hedleys Sandstone Member. See COMMENTS for more.||Siltstone, shale, sandstone.|
17123|South Nicholson Group|67352|4|Described|v,p8,p11,p16-20,p31-32,p41-42,p46-49,p51|Calymmian|Calymmian|Smith and Roberts (1963). South Nicholson Basin. Floors much of the central Georgina Basin. Provisional age from correlation with Roper Group (McArthur Basin). 1552 +/- 165 Ma (Harding in Fisher, 1965).|c.1500 - c.1400 Ma.||Wild Cow and Accident Subgroups.|Overlain (unconformably) by Gum Creek Formation or Helen Springs Volcanics.  Equivalent to Renner Group; correlated with Roper Group.|Siliciclastic sedimentary rocks.|
17123|South Nicholson Group|67499|5|Briefly described|p940, p947, p942 Fig.4, p949|Calymmian|Calymmian|Age of basal units determined using SHRIMP U-Pb dating of zircons in tuff layers. Group said to be hematitic and iron rich.|1493 +/- 8 Ma||Includes Quamby Conglomerate?|Overlies McNamara Group.||
17123|South Nicholson Group|67539|5|Briefly described|p14, p15, p16||||||Includes Boodjamulla Formation, Hedleys Sandstone, Pandanus Siltstone, Burangoo Sandstone, Wallis Siltstone, Constance Sandstone, Mullera Formation, Tidna Sandstone.|Unconformably underlain by the McNamara Group.||
17123|South Nicholson Group|68020|5|Briefly described|p128|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Includes oolitic Fe deposits.|||?Includes Mullera Formation?|||
17123|South Nicholson Group|68146|5|Briefly described|p2, p5, p21, p28-29, p35, p196-198|Proterozoic|Proterozoic|Currently accepted (tentative) age is based on correlation with c.1500-1400 Ma Roper Group in NT. Age determinations in this study do not provide an improved understanding of the depositional ages of the Group.|||Wild Cow, Accident Subgroups.|Unconformably overlies Doomadgee Formation (Fickling Group). Correlated with the Roper Group.|Siliciclastic sediments.|
17123|South Nicholson Group|68542|6|Mentioned|p6|||||||Overlies Upper McNamara Group||
17123|South Nicholson Group|68553|6|Mentioned|Map legend; schematic diagram.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||||
17123|South Nicholson Group|68575|5|Briefly described|p3, p11, p19, p27-33, p125, p128|||South Nicholson Basin. Maximum depositional age of 1602 +/- 22 Ma (from basal Hedleys Sandstone), but post-dates the 1550-1500 Ma Isan Orogeny.|<1500 Ma.||Wild Cow Subgroup; Tidna, Hedleys Sandstones.|||
17123|South Nicholson Group|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||||Unconformably overlies McNamara Group.||
17123|South Nicholson Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|South Nicholson/Lawn Hill Basin.|||||Predominantly shallow marine sandstones.|12-JUL-16
17123|South Nicholson Group|69423|6|Mentioned|p8:4 Fig.8.7|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||||12-JUL-16
17123|South Nicholson Group|69430|5|Briefly described|p15:26|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Correlated with Roper Group (McArthur Basin).||12-JUL-16
17123|South Nicholson Group|69433|6|Mentioned|p18:4, 10|||South Nicholson Basin.||||Unconformably overlies Doomadgee Formation (Fickling Group), McNamara and Benmara Groups, Lawn Hill Platform.||12-JUL-16
17123|South Nicholson Group|69434|4|Described|p19:2-7|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Correlated with the Roper Group, dated at 1492 +/- 4 Ma.|1500-1400 Ma.||Accident and Wild Cow Subgroups.|Unconformably overlies Murphy Metamorphics, McNamara and (probably) Benmara Groups. Is overlain unconformably by Bukalara Sandstone, Wonarah Formation and Helen Springs Volcanics.||12-JUL-16
17123|South Nicholson Group|69443|5|Briefly described|p28:5, 12, 21-22|Calymmian|Mesoproterozoic|South Nicholson Basin.||||Is overlain unconformably by Bukalara Sandstone and Wonarah Formation /Barkly Group (also ?disconformably). Correlative of Renner Group.||12-JUL-16
17123|South Nicholson Group|69445|5|Briefly described|p30:5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Overlain unconformably by Peaker Piker Volcanics (now Helen Springs Volcanics). Is overlain unconformably by Colless Volcanics.||12-JUL-16
17123|South Nicholson Group|69591|5|Briefly described|p27, p29, p52-54, p88, p111|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin, Mount Isa Province. Age is not certain: probably Calymmian to Ectasian. The correlate (Mainoru Formation) has been dated at 1492 +/- 4 Ma. Deformed into a series of domes and basins, and cut by E- to ENE-trending faults, with minor local thrusting.|||Wild Cow, Accident Subgroups.|Is overlain unconformably by Bukalara Sandstone. Correlated with Roper Group, and Mainoru Formation in NT.||
17123|South Nicholson Group|69673|6|Mentioned|p56, p57|||Age is based on correlation with Roper Group.|1500-1400 Ma||Includes Wild Cow Subgroup, Accident Subgroup|Correlated with Roper Group.||
17123|South Nicholson Group|69928|6|Mentioned|p224|Mesoproterozoic|Mesoproterozoic|Mount Isa region. Postulated deposition resulting from Anmatjira Event (1500-1400 Ma) in the Arunta Inlier.||||||
17123|South Nicholson Group|70822|6|Mentioned|p104|||||||Correlated with Roper Group||
17123|South Nicholson Group|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.|||Constance, Mittiebah Sandstones; Mullera Formation.|Unconformably overlies Fickling Group. Is overlain unconformably by Bukalara Sandstone.|Sandstone, siltstone, greywacke.|
17123|South Nicholson Group|70897|4|Described|p36-48 and Figs.1.7.1-9|Mesoproterozoic|Mesoproterozoic|Preserved over c. 20 000 km2 in far NW QLD and adjacent NT. Highly variable thickness to over 2000m: evidence suggests positive basement relief during early stages of deposition of this unit. Thickens to S and SW.|||Constance Sandstone; Pandanus, Wallis, Bowthorn, Train Range Ironstone, Members.|Roper Superbasin. Unconformably overlies McNamara Group and all units of the Fickling Group. Broadly correlated with Roper Group.|Quartz sandstone interstratified with siltstone and shale. Mainly medium- to coarse-grained, fluvial and shallow-marine quartz sandstone in lower half; deeper marine, finer-grained lithologies (glauconitic sandstone, siltstone, shale) in upper half.|
17123|South Nicholson Group|70968|5|Briefly described|v, p2-3, p131 Fig.118, p132, p137|Ectasian|Calymmian|South Nicholson Basin. Not included in this study. Probable correlative of the Winton package (i.e. Roper, Tijunna and Renner Groups). Up to 6500m thick.|||Accident, Wild Cow Subgroups.|||
17123|South Nicholson Group|71059|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||||Equivalent to the Roper Group.||
17123|South Nicholson Group|71369|4|Described|p1-p2, p4-8, p10, p12, p23, p46-50|Ectasian|Calymmian|South Nicholson Basin. Composite measured sections. Faulting and folding after ~1324 Ma described in some detail. Geologic history summarised.|||Wild Cow, Accident Subgroups.|Unconformably overlies McNamara and Fickling Groups. Correlated with Roper Group.|The lower half is predominantly thick-bedded, well-indurated sandstone; the upper half is mainly thinly-bedded or laminated mudstone.|20-FEB-18
17123|South Nicholson Group|71488|6|Mentioned|p142|||South Nicholson Basin.||||||
17123|South Nicholson Group|71502|6|Mentioned|p2|||||||||
17123|South Nicholson Group|71606|5|Briefly described|p137|Calymmian|Calymmian|South Nicholson Basin.||||Underlain unconformably by Fickling Group.||
17123|South Nicholson Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.|||||Quartzose sandstone, siltstone, shale.|
17123|South Nicholson Group|72297|5|Briefly described|p712|||South Nicholson Basin.|||Train Range Ironstone Member.|||
17123|South Nicholson Group|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.|||Includes Accident Subgroup and Wild Cow Subgroup.|||
17123|South Nicholson Group|72418|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72421|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72422|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72423|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.|||Includes Accident Subgroup, Wild Cow Subgroup.|||
17123|South Nicholson Group|72526|5|Briefly described|p1-5, 8, 20, 33, 40, 46,56,67,p85-86|Mesoproterozoic|Mesoproterozoic|Shown as located in the South Nicholson Basin. Inferred to be same age as Roper Group. LA-ICP-MS maximum depositional ages from undifferentiated borehole samples range from 1540+/-14- Ma to 1510+/-51 Ma.|c. 1500 Ma to 1313 Ma inferred||Wild Cow Subgroup and Accident Subgroup|Shown as partially and unconformably overlying Benmara Group, Fickling Group and McNamara Group.||
17123|South Nicholson Group|72527|4|Described|p1, p3, p10-12, p20, p27, p34, p41.|Mesoproterozoic|Mesoproterozoic|No tuffs identified in this Group, so no direct age constraints, only maximum depositional ages. Maximum age from underlying units: 1589+/-3 Ma. Maximum depostional ages range between 1750 and 1570 Ma. Best estimates on depositional age range is 1500-1400 Ma. See also p49, p56, p63, p71, p78, p86, p119, p140, p161, p193, p195-196.|c. 1500-1400 Ma.||Accident Subgroup and Wild Cow Subgroup.|Unconformably overlies McNamara Group, Nathan Group, Fickling Group, Surprise Creek Formation.||
17123|South Nicholson Group|72889|6|Mentioned|p6 Fig.i.|||||||||
17123|South Nicholson Group|72912|4|Described|p5 Fig.3, p12-15, p20-26.|Mesoproterozoic|Mesoproterozoic|Present in the Carrara Sub-basin. Seismically imaged in Murphy Province, Calvert Superbasin equivalent and under Georgina Basin sediments. Considered to be part of the Roper Superbasin. See also p33 Fig.12, p34-35, p45-49.|||Accident Subgroup and Wild Cow Subgroup.|Shown as unconformably overlying Benmara and Fickling Groups,and overlying McNamara Group. Correlated with Roper Group.|Includes siltstone, sandstone, dolomitic siltstone, ironstone.|15-MAR-21
17123|South Nicholson Group|72913|5|Briefly described|p7, p9.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern part of the South Nicholson Basin.|||Wildcow Subgroup and Accident Subgroup|Shown as overlying Fickling Group, McNamara Group.|Includes sandstone, siltstone,|
17123|South Nicholson Group|72919|6|Mentioned|p. 1, 3, 5, 24-25, 31-32, 34-36, 39...|Ectasian|Calymmian|There are considerable 'cross-border' discrepancies between stratigraphic frameworks for this unit in the NT and QLD. May include the Caufield beds. Deposition bracketed to between ca. 1483-1470 Ma and ca. 1266 Ma based on comprehensive SHRIMP U-Pb zircon and xenotime geochronology presented by Anderson et al. (2019a, b) and Kositcin and Carson (2019). This data supports temporal correlation with the Roper Group. Two new U-Pb SHRIMP zircon maximum depositional ages of 1605 +/- 18 Ma and 1610 +/- 35 Ma were presented herein for unnamed sandstones from undifferentiated intervals of this unit. These were interpreted a probably belonging to the Constance Sandstone or equivalent. More locations: p. 41-43, 47, 56-57, 63-64, 70, 77, 85-86, 93-95.|Between ca. 1483-1470 Ma and ca. 1266 Ma||Accident Subgroup, Wild Cow Subgroup and units therein|Unconformably underlain by Widdallion Sandstone Member (McNamara Group). Unconformably overlain by Bukalara Sandstone.||
17123|South Nicholson Group|72967|6|Mentioned|p2, p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.|||Mullera Formation, Constance Sandstone, Mittebah Sandstone|||
17123|South Nicholson Group|73042|6|Mentioned|p1, p2, p4, p6-7, p9|Ectasian|Calymmian|South Nicholson Basin region, Roper Superbasin. Geochronological constraint based on U-Pb zircon and xenotime age data of Anderson et al. (2019) and Carson et al. (2020). See also p9, p11, p14.|ca 1483 Ma and ca 1266 Ma||Accident Subgroup and Wildcow Subgroup, and units therein.|Unconformably underlain by the Doomadgee Formation (Fickling Group).||23-JUN-22
17123|South Nicholson Group|73043|6|Mentioned|p7 Fig.2|Mesoproterozoic|Mesoproterozoic||||Includes Constance Sandstone, Top Lily Sandstone.|||
17123|South Nicholson Group|73083|6|Mentioned|p6, p9, p22, p34-35, p39, p44, p69, p71|||Extend southward beneath the Georgina Basin. Includes sedimentary iron occurrences of the 'Constance Range type' composed of hematite, chamosite, and siderite, in places enriched by lateritic weathering. Mostly of uniform and very low magnetisation.|||Wild Cow Subgroup, Crow Formation, Mittiebah Sandstone||Includes siliciclastics.|
17123|South Nicholson Group|73098|6|Mentioned|p5|||South Nicholson region. Overlies sedimentary package composed of the Paleoproterozoic Isa Superbasin.||||||
17123|South Nicholson Group|73144|6|Mentioned|p8, p13, p19, p23, p43-44, p47-49|Calymmian|Calymmian|South Nicholson Basin. Fluvial to shallow marine. May be similar in age to the Roper Group.|||Accident and Wild Cow subgroups, Tidna, Elizabeth, Constance, Burangoo, and Hedleys sandstones, Mullera, Wallis, and Pandanus formations, and members therein|||
17123|South Nicholson Group|73412|6|Mentioned|p3, 8, 18|||||||Lateral equivalent to the Roper Group.||
17135|Southlands Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
17135|Southlands Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
17135|Southlands Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Lower Cretaceous to Upper Jurassic||||||
17135|Southlands Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic to Lower Cretaceous||||||
17135|Southlands Formation|30695|4|Described|Table 4|||Upper Jurassic-Lower Cretaceous age||||||
17135|Southlands Formation|30702|5|Briefly described|p50|||See also Fig.1. Stratigraphic table.||||||
17135|Southlands Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
17135|Southlands Formation|39445|5|Briefly described|Table 10|||||||||
17135|Southlands Formation|40666|6|Mentioned|p353|||||||||
17135|Southlands Formation|43008|5|Briefly described|map legend|||||||||
17135|Southlands Formation|44022|14|Not recorded|Map Legend|Cretaceous|Jurassic|||||||
17135|Southlands Formation|44023|4|Described|Tb.3,p12|Cretaceous|Jurassic|||||||
17135|Southlands Formation|45071|3|Fully described|Table 15|||Refers Mollan et al. (1971). Equivalent Orallo Formation||||||
17135|Southlands Formation|48919|2|Defined|p67|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
17135|Southlands Formation|64856|5|Briefly described|p96|||Lower part grades into Orallo Formation in western Surat Basin, north of Muckadilla, then interfingers with Hooray Sandstone NW of Mitchell.|| ||||31-JAN-13
17135|Southlands Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Bungil Formation.||
17135|Southlands Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil and Orallo Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
17135|Southlands Formation|69594|6|Mentioned|p537|||||||Grades into underlying Orallo Formation. Interfingers with lower Hooray Sandstone.||
17135|Southlands Formation|70821|5|Briefly described|p80|||Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Bungil Formation.||
17135|Southlands Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||||Overlies Gubberamunda Sandstone. Is overlain by Bungil FZ.||
17143|Spear Siltstone|23397|5|Briefly described|p469|||||||||
17143|Spear Siltstone|23398|5|Briefly described|p454|||Of Mount Isa Group.||||||
17143|Spear Siltstone|23399|4|Described|p495|||Of Mount Isa Group.||||||01-SEP-08
17143|Spear Siltstone|23408|4|Described|p512, p513 Fig. 2|||Of Mount Isa Group. Rhythmically laminated dolomitic siltstone in the upper section. Also this unit contains stromatolites, halite pseudomorphs, flat pebble conglomerates and x-bedded chammel deposits.||||||15-JUN-09
17143|Spear Siltstone|23961|6|Mentioned|p1192 Fig. 3|||Geological Province: Mt Isa Inlier.||||||
17143|Spear Siltstone|23969|6|Mentioned|p1379 Fig.6|||Geological Province: Mount Isa Inlier.||||||02-MAR-05
17143|Spear Siltstone|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: Mount Isa Group||||||07-NOV-08
17143|Spear Siltstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Mount Isa Group. Overlain by Magazine Shale. Geological Province: Leichardt River Fault Trough.||||||25-FEB-05
17143|Spear Siltstone|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group.  Overlies the Urquhart Shale; underlies Kennedy Siltstone.||||||25-AUG-04
17143|Spear Siltstone|30535|6|Mentioned|p403|||Refers Bennett(1965). See type sections P405||||||
17143|Spear Siltstone|31207|6|Mentioned|Table 1|||||||||
17143|Spear Siltstone|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17143|Spear Siltstone|32041|4|Described|p355|||||||||
17143|Spear Siltstone|32042|4|Described|p43|||||||||
17143|Spear Siltstone|32660|5|Briefly described|Table 5|||||||||
17143|Spear Siltstone|32959|6|Mentioned|Fig.21|||||||||
17143|Spear Siltstone|33900|5|Briefly described|p14|||||||||
17143|Spear Siltstone|34321|6|Mentioned|p55|||See also P56. Diagrams||||||
17143|Spear Siltstone|34499|6|Mentioned|Table 1|||||||||
17143|Spear Siltstone|34754|6|Mentioned|p42|||||||||
17143|Spear Siltstone|35074|6|Mentioned|Fig.2|||||||||
17143|Spear Siltstone|35116|6|Mentioned|Table.4|||||||||
17143|Spear Siltstone|35881|6|Mentioned|Fig.2|||||||||
17143|Spear Siltstone|39445|5|Briefly described|Table 2|||||||||
17143|Spear Siltstone|39561|6|Mentioned|Fig.10|||||||||
17143|Spear Siltstone|39602|6|Mentioned|p619|||||||||
17143|Spear Siltstone|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
17143|Spear Siltstone|41248|6|Mentioned|Fig.7|||||||||
17143|Spear Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
17143|Spear Siltstone|42072|6|Mentioned|Fig.1 P1615|||||||||
17143|Spear Siltstone|42350|6|Mentioned|Fig.1 P543|||||||||
17143|Spear Siltstone|42782|6|Mentioned|p458|||of Mount Isa Group||||||
17143|Spear Siltstone|43760|6|Mentioned|p441|||||||||
17143|Spear Siltstone|44517|2|Defined|p235,236,244,map||Paleoproterozoic|Unit of Mount Isa Group.||||||07-NOV-08
17143|Spear Siltstone|44684|14|Not recorded|p3|||||||||
17143|Spear Siltstone|44685|14|Not recorded|p75|||||||||
17143|Spear Siltstone|44843|14|Not recorded|p175|||||||||
17143|Spear Siltstone|45072|5|Briefly described|p35|||Chem. anal. Table 9||||||
17143|Spear Siltstone|45136|5|Briefly described|p50|||||||||
17143|Spear Siltstone|45166|5|Briefly described|p28|||||||||
17143|Spear Siltstone|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
17143|Spear Siltstone|50332|5|Briefly described|p21|Proterozoic|Proterozoic|Of the Mount Isa Group. Underlain by Urquhart Shale. Geological Province: Western Fold Belt Province. Contains laminated dolomitic siltstone and shale.||||||07-FEB-11
17143|Spear Siltstone|50624|5|Briefly described|p237 Fig.4||Statherian|Parent: Mount Isa Group. Overlies Urquhart Shale.||||||24-NOV-04
17143|Spear Siltstone|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Overlain by Kennedy Siltstone, underlain by Urquhart Shale. Geological Province: Western Fold Belt.||||||
17143|Spear Siltstone|61923|5|Briefly described|p30 Fig.3|||||||||
17143|Spear Siltstone|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1652+/-7Ma. Geological Province: Isa Superbasin, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
17143|Spear Siltstone|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Mount Isa. Shown as Spear Slst.||Mount Isa Group|||Variably dolomitic organic siltstones and shales.|
17143|Spear Siltstone|62535|5|Briefly described|p672, p674|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.||Mount Isa Group.||||
17143|Spear Siltstone|63866|5|Briefly described|p59|||Isa Superbasin.||Gun Supersequence||||
17143|Spear Siltstone|64367|6|Mentioned|p573 Fig. 2|||||||||07-FEB-11
17143|Spear Siltstone|67026|6|Mentioned|p336 Fig.3. |Proterozoic|Proterozoic|||||||
17143|Spear Siltstone|67323|5|Briefly described|GIS attrib tbl, p26, p34|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Isa Superbasin.|~1660-1650 Ma.|Mount Isa Group.|||Laminated dolomitic siltstone and shale.|
17143|Spear Siltstone|68542|6|Mentioned|p6|||||||Overlies Urquhart Shale, overlain by Kennedy Siltstone||
17143|Spear Siltstone|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Urquhart Shale. Is overlain by Kennedy Siltstone.||
17143|Spear Siltstone|68732|6|Mentioned|p160, p162, p163|||||||||
17143|Spear Siltstone|69591|5|Briefly described|p43 Fig.2.31, p45, p55|||Leichhardt Domain, Isa Superbasin. Part of Gun Supersequence. Deposited below storm base.||Mount Isa Group.|||Laminated dolomitic siltstone and shale.|
17143|Spear Siltstone|70282|6|Mentioned|p544 Fig.1, p546|||Presented as Kennedy-Spear Siltstone.||||||13-FEB-18
17143|Spear Siltstone|73525|6|Mentioned|p4-5 Fig.2|||Leichhardt River Domain.|||||Carbonates.|
17149|Speed Creek Granite|23422|5|Briefly described|p181, p218 Table 6.12|Permian|Permian|Of Leichhardt Supersuite.||||||
17149|Speed Creek Granite|23509|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
17149|Speed Creek Granite|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 179. I-Type.||||||
17149|Speed Creek Granite|23893|5|Briefly described|p18|Permian|Late Carboniferous|||||||
17149|Speed Creek Granite|42689|5|Briefly described|map legend|Early Permian|Carboniferous|Reserved as Speed Creek Granodiorite.||||||
17149|Speed Creek Granite|43095|2|Defined|p80|Early Permian|Late Carboniferous|K-Ar age of 284 - 296 Ma.||||||
17149|Speed Creek Granite|43259|4|Described|Appendix 1,p28.|Early Permian|Late Carboniferous|K-Ar mineral ages are 284 to 296 Ma.||||||
17149|Speed Creek Granite|43589|2|Defined|p24, p25 appdx.|Early Permian|Late Carboniferous|Age: 283+/-4 Ma (U-Pb SHRIMP)||||||27-AUG-14
17149|Speed Creek Granite|66529|5|Briefly described|p24 |Permian|Late Carboniferous|Minimum age is Early Permian. Age is of a single analysis of a detrital zircon.||||Intrudes Insolvency Gully Formation.||
17149|Speed Creek Granite|68419|5|Briefly described|Map Legend|Permian|Permian|Of the Kennedy Province. Shown as Early Permian age. Includes an informal unnamed subunit.|||||Grey to cream, fine to coarse-grained, equigranular biotite granite; grey to cream, fine to coarse-grained, equigranular to slightly porphyritic biotite granite.|
17149|Speed Creek Granite|68420|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Kennedy Province. Includes an informal unnamed subunit.|||||Grey to cream, fine to coarse-grained, equigranular biotite granite; grey to cream, fine to coarse-grained, equigranular to slightly porphyritic biotite granite.|
17149|Speed Creek Granite|69593|5|Briefly described|p494|Permian|Late Carboniferous|Paluma Subprovince, Kennedy Igneous Association. Charters Towers-Townsville area.|~310-283 Ma.|Leichhardt Supersuite.|||Hornblende-biotite and biotite granite and granodiorite.|
17159|Spicers Gap Trachyte Member|39969|6|Mentioned|p9|||||||||
17159|Spicers Gap Trachyte Member|48917|6|Mentioned|p7|||Refers Stevens (1965)||||||
17159|Spicers Gap Trachyte Member|73450|6|Mentioned|p92|||Of Stevens, 1965; Grenfell, 1984; Ewart & Grenfell, 1985. Never described in detail.||Governors Chair Volcanics|||Felsic.|29-SEP-22
17179|Splinter Creek Formation|30451|4|Described|p26|||||||||
17179|Splinter Creek Formation|31586|6|Mentioned|p4|||||||||
17179|Splinter Creek Formation|31587|6|Mentioned|p60|||Distribution of Lithostrotion||||||
17179|Splinter Creek Formation|31659|6|Mentioned|p54|||Part of Caswell Creek Gp.||||||
17179|Splinter Creek Formation|32866|6|Mentioned|p22|||Fossil content||||||
17179|Splinter Creek Formation|33728|6|Mentioned|p52|||||||||
17179|Splinter Creek Formation|33774|6|Mentioned|p19|||Strat.||||||
17179|Splinter Creek Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
17179|Splinter Creek Formation|34155|6|Mentioned|p94|||Lower Carboniferous. Caswell Creek Group.||||||
17179|Splinter Creek Formation|39445|5|Briefly described|Table 6|||||||||
17179|Splinter Creek Formation|42547|4|Described|p50|||See also [typo] Creek Formation.||||||
17179|Splinter Creek Formation|44360|2|Defined|p1-4,7,8,10,12,21,||Visean|p23-27,30,32,33,35,map. Unit of Caswell Creek Group.||||||
17179|Splinter Creek Formation|44379|14|Not recorded|p15|||Ref. to Tom McKellar 1967||||||
17179|Splinter Creek Formation|44487|14|Not recorded|p199|||Ref. to McKellar 1967.||||||
17179|Splinter Creek Formation|45097|6|Mentioned|p23|||Fossils. Correlation chart||||||
17179|Splinter Creek Formation|46803|6|Mentioned|p143|||See also Fig. 4||||||
17179|Splinter Creek Formation|70050|5|Briefly described|p327, p341, p366|Visean|Visean|Monto area. Contains Cionodendron coral fossils.|||Kolonga Creek Limestone Member.|||16-APR-18
17180|Split Rock Sandstone|22954|6|Mentioned|Fig3p9|||||||||
17180|Split Rock Sandstone|23031|4|Described|31|||Geological province: Georgina Basin. Underlain by Mail Change Limestone, V-Creek Limestone, Age Creek Formation.||||||04-DEC-06
17180|Split Rock Sandstone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|Geological Province: Georgina Basin.||||||
17180|Split Rock Sandstone|30479|6|Mentioned|Fig.7|||Stratigraphic relationships||||||
17180|Split Rock Sandstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17180|Split Rock Sandstone|31287|6|Mentioned|p430|||Refers Opik (1956).||||||04-DEC-06
17180|Split Rock Sandstone|31396|6|Mentioned|Fig.3|||||||||
17180|Split Rock Sandstone|33111|4|Described|p42|||Mention p28.||||||04-DEC-06
17180|Split Rock Sandstone|34287|6|Mentioned|Fig.3|||||||||
17180|Split Rock Sandstone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
17180|Split Rock Sandstone|35054|6|Mentioned|Table 23|||||||||
17180|Split Rock Sandstone|35553|6|Mentioned|p153|||||||||
17180|Split Rock Sandstone|37572|4|Described|p158|||See also Fig.7 and p165.||||||04-DEC-06
17180|Split Rock Sandstone|38444|6|Mentioned|p139|||||||||
17180|Split Rock Sandstone|38446|6|Mentioned|Table 23|||||||||
17180|Split Rock Sandstone|39445|5|Briefly described|Table 4|||See also p62.||||||04-DEC-06
17180|Split Rock Sandstone|39690|6|Mentioned|Table 1|||||||||
17180|Split Rock Sandstone|40856|6|Mentioned|Fig.23.6|||||||||
17180|Split Rock Sandstone|41129|6|Mentioned|Fig.8|||||||||
17180|Split Rock Sandstone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
17180|Split Rock Sandstone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
17180|Split Rock Sandstone|44205|14|Not recorded|p51,155|||See also Lexicon.||||||
17180|Split Rock Sandstone|44206|14|Not recorded|p122|||Overlies Pilpah Sandstone.||||||
17180|Split Rock Sandstone|44210|2|Defined|map,p5,7,15,Tb.2||Middle Cambrian|||||||
17180|Split Rock Sandstone|44211|2|Defined|p92,101-107|||Erosional residuals in Undilla Basin partly covered by Polland Shale.||||||04-DEC-06
17180|Split Rock Sandstone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
17180|Split Rock Sandstone|44275|14|Not recorded|Map Legend|||||||||
17180|Split Rock Sandstone|44920|14|Not recorded|Map Legend, Sheet 2||Middle Cambrian|||||||
17180|Split Rock Sandstone|44989|14|Not recorded|p.122|||Overlies Pipah Sandstone.||||||
17180|Split Rock Sandstone|45052|3|Fully described|p94|||M.Camb.||||||
17180|Split Rock Sandstone|45054|6|Mentioned|p5|||Fossil locality||||||
17180|Split Rock Sandstone|45079|5|Briefly described|p38|||Cambrian age||||||
17180|Split Rock Sandstone|45119|6|Mentioned|p3|||||||||
17180|Split Rock Sandstone|48906|14|Not recorded|Tb.1|||||||||
17180|Split Rock Sandstone|64068|5|Briefly described|p62, 64, 225|||Eastern Georgina Basin. Correlated with Arthur Creek Formation, Roaring Siltstone, Devoncourt Limestone.||||||
17180|Split Rock Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies Age Creek Formation and Mail Change Limestone.|Fine-grained quartzose arenite, siltstone.|
17180|Split Rock Sandstone|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||||12-JUL-16
17180|Split Rock Sandstone|69573|6|Mentioned|p659, 665|||Georgina Basin. Contains Drumian Stage [Cambrian] fossil sites. High energy, inner shelf setting.||||||
17180|Split Rock Sandstone|69591|5|Briefly described|p87, p90, p96-97|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Preserved as erosional residuals in the Undilla area. Contains trilobites.||Narpa Group.||Conformably overlies Age Creek Formation. Overlies Mail Change Limestone conformably, locally disconformably, or grades laterally into it. Is overlain unconformably by Polland Waterhole Formation.|Fine quartz sandstone with siltstone interbeds and local cross-bedding.|
17180|Split Rock Sandstone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stage: Undillan.||of Narpa Group.||||
17180|Split Rock Sandstone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
17180|Split Rock Sandstone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Mail Change Limestone|Sandstone.|
17205|Springbok Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499|Oxfordian|Oxfordian|N Surat Basin. 50-150m thick.||Unit in Injune Creek Group.||Equivalent to Adori and Pilliga Sandstones and basal Kumbarilla beds.|Mainly cross-bedded labile sandstone, with carbonaceous siltstone and mudstone, and rare thin coal and bentonite lenses.|
17205|Springbok Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Jurassic|Late Jurassic|In Surat Basin, Eromanga Basin.||||||
17205|Springbok Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Middle Jurassic|275 m. Surat Basin||||||
17205|Springbok Sandstone|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig.22.8|Callovian|Bathonian|Of the Injune Creek Group. Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|22865|5|Briefly described|Table22.1p296-7|Callovian|Bathonian|||||||
17205|Springbok Sandstone|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
17205|Springbok Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|24068|4|Described|p270 Table 2|Late Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 150m.||||||
17205|Springbok Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|29591|6|Mentioned|Table 15|||||||||
17205|Springbok Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|30694|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
17205|Springbok Sandstone|30695|4|Described|Table 4|||Middle-Upper Jurassic||||||
17205|Springbok Sandstone|30696|4|Described|Table 4|||Middle-Upper Jurassic||||||
17205|Springbok Sandstone|30699|6|Mentioned|p53|||Stratigraphy. Middle Jurassic-Early Cretaceous age||||||
17205|Springbok Sandstone|30701|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper JurassicM - U||||||
17205|Springbok Sandstone|30702|4|Described|p48|||See also P50-52,Fig.1,2. Stratigraphic table||||||
17205|Springbok Sandstone|31121|6|Mentioned|p389|||||||||
17205|Springbok Sandstone|32138|6|Mentioned|p396|||||||||
17205|Springbok Sandstone|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|32276|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.M - U||||||
17205|Springbok Sandstone|32797|6|Mentioned|Table 4|||M.-U. Jur.||||||
17205|Springbok Sandstone|33070|4|Described|Table 2|||M.-U.Jur.||||||
17205|Springbok Sandstone|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33090|4|Described|Table 4|||Mid.-U.Jur.||||||
17205|Springbok Sandstone|33091|5|Briefly described|p10|||Strat.||||||
17205|Springbok Sandstone|33094|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33367|3|Fully described|p23|||||||||
17205|Springbok Sandstone|33371|4|Described|p58|||||||||
17205|Springbok Sandstone|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33672|6|Mentioned|p44|||||||||
17205|Springbok Sandstone|34613|4|Described|Table 4|||||||||
17205|Springbok Sandstone|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
17205|Springbok Sandstone|35663|6|Mentioned|p129|||||||||
17205|Springbok Sandstone|35937|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|36243|6|Mentioned|Table 7A|||||||||
17205|Springbok Sandstone|36570|6|Mentioned|p55|||||||||
17205|Springbok Sandstone|37117|5|Briefly described|p313|||||||||
17205|Springbok Sandstone|37993|6|Mentioned|p159|||||||||
17205|Springbok Sandstone|37994|6|Mentioned|p146|||||||||
17205|Springbok Sandstone|37995|4|Described|p64|||||||||
17205|Springbok Sandstone|37997|6|Mentioned|p86|||||||||
17205|Springbok Sandstone|39212|5|Briefly described|p16|||||||||
17205|Springbok Sandstone|39445|5|Briefly described|Table 10|||||||||
17205|Springbok Sandstone|39494|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|39943|6|Mentioned|Table 9A|||||||||
17205|Springbok Sandstone|40030|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|40245|6|Mentioned|Table 2|||||||||
17205|Springbok Sandstone|40249|6|Mentioned|p38|||||||||
17205|Springbok Sandstone|40250|6|Mentioned|Fig.7|||||||||
17205|Springbok Sandstone|40540|6|Mentioned|Fig.2|||||||||
17205|Springbok Sandstone|40541|3|Fully described|p109|||||||||
17205|Springbok Sandstone|40544|6|Mentioned|Fig.6|||||||||
17205|Springbok Sandstone|40666|4|Described|p357|||||||||
17205|Springbok Sandstone|41060|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41064|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41187|6|Mentioned|Fig.2|||||||||
17205|Springbok Sandstone|41188|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41210|5|Briefly described|Fig.3|||||||||
17205|Springbok Sandstone|41216|6|Mentioned|Fig.18|||||||||
17205|Springbok Sandstone|41247|6|Mentioned|Fig.7|||||||||
17205|Springbok Sandstone|41266|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41992|4|Described|Fig.2 P183|||||||||
17205|Springbok Sandstone|42007|5|Briefly described|Fig.2 P182|||Misspelling of Springbok?||||||
17205|Springbok Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
17205|Springbok Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
17205|Springbok Sandstone|43000|5|Briefly described|Fig.5,p112|||Of Injune Creek Group.||||||16-SEP-08
17205|Springbok Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
17205|Springbok Sandstone|44171|4|Described|p194,195,197,198|||Upgraded from Springbok Sandstone Lens.||||||
17205|Springbok Sandstone|45110|2|Defined|p95|Middle Jurassic|Middle Jurassic|Formerly Springbok Sst. Lens (Exon,1966) & Springbok Sst. Mbr. See also p24.||||||11-DEC-15
17205|Springbok Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
17205|Springbok Sandstone|46984|6|Mentioned|Table 1|||||||||
17205|Springbok Sandstone|48917|6|Mentioned|p30|||Stratigraphic relationships||||||
17205|Springbok Sandstone|48919|2|Defined|p61|Middle Jurassic|Middle Jurassic|||||||
17205|Springbok Sandstone|48920|6|Mentioned|Table 7|||See also P50. Refers Power & Devine (1968)||||||
17205|Springbok Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
17205|Springbok Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
17205|Springbok Sandstone|60993|5|Briefly described|p36|Late Jurassic|Middle Jurassic|Comparable in age with Kangaroo Creek Sandstone. May be the equivalent of the lower sandstone section of the Woodenbong beds. Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|61000|5|Briefly described|p186 Fig. 4|Callovian|Bathonian|Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|61005|6|Mentioned|p253|||Contains apatites. Equivalent to Kangaroo Sandstone (intended as Kangaroo Creek Sandstone). See also p255 Figs. 23, 24 and 25.||||||
17205|Springbok Sandstone|61377|5|Briefly described|p148 Tb. SU1|Jurassic|Middle Jurassic|Quartz sandstone, minor siltstone and shale. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
17205|Springbok Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Late Jurassic|Geological Province: Surat Basin.||||||13-MAR-09
17205|Springbok Sandstone|63218|6|Mentioned|p211, p212 Fig.3, p217, pp219-221. |Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.|Basal clean, medium- to coarse-grained, quartzose sandstone. Contains thin coal seams with high (46 vol%) inertinite.|
17205|Springbok Sandstone|63979|5|Briefly described|p38|||Underlies Walloon Coal Measures. Intertongues with Adori Sandstone in places. Geological province: Surat Basin.||||||07-FEB-11
17205|Springbok Sandstone|64197|6|Mentioned|p630 Fig.7|Jurassic|Jurassic|Surat Basin.||||Underlies Westbourne Formation; overlies Walloon Coal Measures.||
17205|Springbok Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Late Jurassic|Late Jurassic|Surat Basin. Equivalent to the Adori Sandstone (Eromanga Basin).||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|64856|3|Fully described|p79, p88-93|Oxfordian|Callovian|Originally the Springbok Sandstone Lens of Exon (1966) in uppermost Birkhead Formation. Superseded by Springbok Sandstone Member (Exon et al., 1967), then the Springbok Sandstone (Power and Devine, 1968). Surat Basin. Type section is the interval 38-50m in BMR Mitchell 3. Conformably overlies Walloon Coal Measures. Laterally equivalent to Adori Sandstone in the Eromanga Basin. Lower part equivalent to the Proud Sandstone. Interfingers with Pilliga Sandstone to the south. Up to 157m thick. Age from palynofloral unit APJ5.|| ||||29-NOV-17
17205|Springbok Sandstone|64857|5|Briefly described|p133, p113 Fig.3|||Surat Basin. Overlies Walloon Coal Measures. Wireline log suggests disconformity.||||||
17205|Springbok Sandstone|64858|6|Mentioned|p182 Fig.3|||||||||30-NOV-09
17205|Springbok Sandstone|65003|5|Briefly described|p8||Jurassic|Of Surat Basin.||||||
17205|Springbok Sandstone|65096|5|Briefly described|p368, p370 Fig.2|Middle Jurassic|Middle Jurassic|Surat Basin?||||Unconformably overlies the Walloon Coal Measures.||
17205|Springbok Sandstone|65112|5|Briefly described|p323; p328; Fig 11 p 324; fig 16 p328|Jurassic|Jurassic||158-157 Ma.|||Underlies the Westbourne Formation, overlies the Walloon Coal Measures.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
17205|Springbok Sandstone|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Late Jurassic|Overlies the Walloon CM, underlies the Westbourne Formation.||||||
17205|Springbok Sandstone|65114|5|Briefly described|p385 Fig.3|Late Jurassic||||||||
17205|Springbok Sandstone|65116|5|Briefly described|Fig 2 p437|Late Jurassic|Late Jurassic|Underlies the Westbourne Formation, Overlies the Walloon Coal Measures, Surat Basin.||||||
17205|Springbok Sandstone|65117|5|Briefly described|p461, 462, 470-472,Table 1 p466|Oxfordian|Oxfordian|Surat Basin, Potential reservoir unit. Some scouring observed at base, so at least disconformable on Walloon Coal Measures. Feldspathic to lithic sandstone, minor siltstone, mudstone and coal. Max thickness 250m.||||||
17205|Springbok Sandstone|65119|6|Mentioned|Fig 13 p520, Fig 14 p521|||Present in the Rockwood 1 and Flinton 1 wells.||||||07-MAR-12
17205|Springbok Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|66915|5|Briefly described|p6 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||||
17205|Springbok Sandstone|67133|5|Briefly described|p2, p5, p14-15, p19-21|Jurassic|Jurassic|21 samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (17-71%) and plagioclase always the dominant feldspar. Kaolinite (5-25%) is the dominant clay mineral. Mixed-layer clays are smectite-dominant.||||Overlies Walloon Subgroup. Is overlain conformably by Westbourne Formation.|Feldspathic sublabile to lithic sandstone, sometimes porous, friable, pebbly or with calcareous cement; andesitic debris and bentonitic tuffs from contemporaneous volcanism.|
17205|Springbok Sandstone|67402|5|Briefly described|p43 tbl HPB1|Oxfordian|Oxfordian|Surat Basin. Highly prospective for the storage of carbon dioxide. Deposited primarily in streams. Approximately 116m thick. See also  p146 fig SRT3, p148, p151, p154 fig SRT15/16, p156.||||Unconformably overlies the Walloon Subgroup. Conformably overlain by the Westbourne Formation.|Feldspathic to lithic sandstone commonly with a calcareous cement that is commonly interbedded with siltstone and mudstone.|
17205|Springbok Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Injune Creek Group.||Overlain by Westbourn Formation. Underlain by Wallon CM.||
17205|Springbok Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|68117|5|Briefly described|p346-347, p349-350|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Juandah Coal Measures (Walloon Subgroup). Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|68135|5|Briefly described|p52 fig 2b, p54|Oxfordian|Oxfordian|Surat Basin (QLD)||||Unconformably overlies Walloon Coal Measures. Overlain by Westbourne Formation|Sandstone.|15-SEP-17
17205|Springbok Sandstone|68139|5|Briefly described|p23-25, p30 Fig.11, p32|Late Jurassic|Late Jurassic|Surat Basin. A major aquifer. In many places, this unit has completely removed the Upper Juandah Coal Measures.||Injune Creek Group.||Unconformably overlies Upper Juandah Coal Measures (Walloon Subgroup). Is overlain unconformably by Westbourne Formation.|Includes volcanic debris and widespread ash-fall tuffs.|
17205|Springbok Sandstone|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|69574|6|Mentioned|p23-24, 26-28, 31-32, 34|Late Jurassic|Late Jurassic|Surat Basin. A major regional aquifer. Thin coal seams have only low gas contents (<2 m3/t).||||Unconformably overlies Walloon Subgroup.||
17205|Springbok Sandstone|69582|5|Briefly described|p36, p38|Late Jurassic|Late Jurassic|Surat Basin.||||Unconformably overlies the Walloon Coal Measures. Overlain by the Westbourne Formation.|Mudstone, sandstone.|
17205|Springbok Sandstone|69594|4|Described|p519, p525, p537, p573|Kimmeridgian|Oxfordian|Exon (1966); Exon et al. (1967). Northern Surat Basin. 12m thick in the type section in BMR Mitchell 3. Maximum thickness of 157m. Fluvial deposits, with increasing overbank and swamp sediments up-section. Volcanic detritus indicates penecontemporaneous volcanism.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain conformably by Westbourne Formation. Laterally continuous with and interfingers with Adori Sandstone.|Dominated by volcanic feldspathic and lithic sandstone with minor pebbly quartzose sandstones near the base and minor interbedded siltstones, mudstones and thin coals in the upper part.|
17205|Springbok Sandstone|69681|6|Mentioned|p74 Fig.3, p82|Late Jurassic|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||Unit in Injune Creek Group.||||
17205|Springbok Sandstone|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Walloon Subgroup. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|69790|5|Briefly described|p1061,p1064-1068, p1070-1072, p1077-1078|||||Unit in Injune Creek Group.||Unconformably overlies Walloon Subgroup. Equivalent to Pilliga Sandstone in NSW.||
17205|Springbok Sandstone|70374|6|Mentioned|p808, p809 figure 1, p812, p813|Kimmeridgian|Oxfordian|Previously considered to be Late Jurassic/Oxfordian, based on biostratigraphy.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain ?conformably by Westbourne Formation.||28-SEP-16
17205|Springbok Sandstone|70725|5|Briefly described|p11, 13-20, 22-25|Late Jurassic|Late Jurassic|Surat Basin. Maceral composition and vitrinite reflectance graphed and discussed. 13C isotope vs. depth tabulated.||Walloon Subgroup.||Unconformably overlies Upper Juandah Coal Measures (Walloon Subgroup).||
17205|Springbok Sandstone|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Surat Basin. Aquifer: generally artesian.||Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|71282|6|Mentioned|p456, p457 Fig.1, p459-460, p462|||Appears as Springbok Formation on p462.||||Unconformably overlies Walloon Subgroup.||
17205|Springbok Sandstone|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
17205|Springbok Sandstone|72297|5|Briefly described|p699 Fig.10.11, p745, p751|Jurassic|Jurassic|Surat Basin. Minor petroleum reserves in fault-related traps.||||Unconformably overlies Walloon Coal Measures or Walloon Subgroup.||
17205|Springbok Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne FZ.||
17205|Springbok Sandstone|72921|5|Briefly described|p15 Fig.2, p50-51|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland.||||Underlies Westbourne Formation and shown as unconformably overlying Walloon Coal Measures.|Includes sandstone and siltstone.|
17205|Springbok Sandstone|73113|5|Briefly described|p. 2, 10, 13, 19, 22-24, 26-27, 29...|||Surat Basin. Groundwater model divides unit into upper and lower layers. Lower portion contains only a small amount of coal. Tight aquifer. More locations: p. 31, 36-37, 41, 49, 51-52, 56-57, 61, 67, 69-70, 75, 78, 80, 88, 94, 98, 116-117, 119, 123, 126-127, 129, 148-149, 152, 158, 160, 162, 165-174, 177-178, 191-193, 199.||||Underlain by Walloon Coal Measures. Overlain by Westbourne Formation.|Lower portions tend to be dominated by coarse to very coarse-grained sandstones; upper portion is typically comprised of fine to coarse-grained, felspathic to lithic sandstone interbedded with siltstone and mudstone.|
17205|Springbok Sandstone|73193|6|Mentioned|p367, p369-370, p372, p375|Kimmeridgian|Kimmeridgian|Surat Basin. Separated from the Walloon Subgroup by the Springbok unconformity.||Injune Creek Group||Unconformably underlain by Walloon Subgroup. Overlain by Westbourne Formation.||
17205|Springbok Sandstone|73200|6|Mentioned|p532 Fig.1, p533, p540|Jurassic|Jurassic|Exposed along the western banks of the Condamine River valley.||||||
17205|Springbok Sandstone|73393|6|Mentioned|p20-21|Tithonian|Tithonian|Surat Basin.||Injune Creek Group||Underlain by Walloon Coal Measures. Overlain by and equivalent to Westbourne Formation.||
17206|Springbrook Rhyolite|39969|6|Mentioned|Fig.22|||||||||
17206|Springbrook Rhyolite|40623|5|Briefly described|p39|||||||||
17206|Springbrook Rhyolite|40896|6|Mentioned|p32|||||||||
17206|Springbrook Rhyolite|42317|5|Briefly described|p2|||||||||
17206|Springbrook Rhyolite|43161|6|Mentioned|13,14|||||||||
17206|Springbrook Rhyolite|69599|5|Briefly described|p631, p633 Fig.8.35, p640, p641 Fig.8.44|||Northern side of the Tweed volcano, centred on Mount Warning. Resistant; forms cliff lines and waterfalls. Table of chemical analyses; REE diagram and comment.||||Approximate equivalent of Nimbin Rhyolite in NSW.|Peraluminous or high-silica rhyolite.|
17206|Springbrook Rhyolite|73450|4|Described|p99-101|||Associated with the Tweed Volcano. Up to 500 m thick. Separated from the Springbrook Rhyolite by basalt (at least locally). Has a glassy base with obsidian and perlite, and a glassy top.|||||Coherent felsic lava and minor pyroclastic deposits including ash flow tuff and ash fall tuff.|
17206|Springbrook Rhyolite|73581|6|Mentioned|p6|||(Stevens 1984). Lies on the northern slope of the Tweed Volcano. Overlies an unnamed basalt within the Binna Burra Rhyolite. Underlies Hobwee Basalt/Blue Knob Basalt.||||||
17227|Springwood Rhyolite|40896|6|Mentioned|p9|||||||||
17229|Square Post Granite|22847|3|Fully described|p 40|Late Ordovician|Ordovician|||||||
17229|Square Post Granite|23509|5|Briefly described|Map Legend|Early Permian|Ordovician|||||||
17229|Square Post Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 110. ?S-Type.||||||
17229|Square Post Granite|23893|6|Mentioned|p13|||||||||
17229|Square Post Granite|42245|2|Defined|p34|Ordovician||Reserved as Square Post Adamellite||||||
17229|Square Post Granite|43093|4|Described|Appendix 1|Late Ordovician|Ordovician|Middle to Late Ordovician||||||
17229|Square Post Granite|43259|4|Described|Appendix 1,p23.||Ordovician|Rb-Sr biotite age is 437+/-5 Ma. Ordovician?||||||
17229|Square Post Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
17242|Staircase Sandstone Member|13516|5|Briefly described|p145 fig 3, p146 fig 4, p150|Early Permian|Early Permian|From Denison Trough, Bowen Basin. Age APP3102 - APP321. See also Staitcase Sandstone Member, p146.||Cattle Creek Formation||||
17242|Staircase Sandstone Member|24077|5|Briefly described|p412 Fig. 8|Early Permian|Early Permian|Of Cattle Creek Formation.  Geological Province: Bowen Basin.||||||
17242|Staircase Sandstone Member|29721|6|Mentioned|p65|||||||||
17242|Staircase Sandstone Member|30826|6|Mentioned|Fig.1|||||||||
17242|Staircase Sandstone Member|31120|4|Described|p150|||||||||
17242|Staircase Sandstone Member|31305|6|Mentioned|p569|||||||||
17242|Staircase Sandstone Member|32139|6|Mentioned|p582|||See Table||||||
17242|Staircase Sandstone Member|32577|4|Described|p23|||L.Perm. See also P24,32,33,42.||||||
17242|Staircase Sandstone Member|32840|6|Mentioned|Fig.2|||Stratigraphy & biostratigraphy||||||
17242|Staircase Sandstone Member|35148|6|Mentioned|p411|||||||||
17242|Staircase Sandstone Member|35150|6|Mentioned|p422|||||||||
17242|Staircase Sandstone Member|35457|6|Mentioned|Fig.4|||l||||||
17242|Staircase Sandstone Member|36243|6|Mentioned|Table 3A|||||||||
17242|Staircase Sandstone Member|36739|6|Mentioned|p19|||||||||
17242|Staircase Sandstone Member|37705|6|Mentioned|Fig.2|||||||||
17242|Staircase Sandstone Member|37726|6|Mentioned|Fig.2|||||||||
17242|Staircase Sandstone Member|39273|6|Mentioned|p305|||||||||
17242|Staircase Sandstone Member|39423|6|Mentioned|p53|||||||||
17242|Staircase Sandstone Member|39943|6|Mentioned|Table 5A|||||||||
17242|Staircase Sandstone Member|41605|6|Mentioned|p29|||See also Fig.2||||||
17242|Staircase Sandstone Member|41920|5|Briefly described|Inside back cover|||||||||
17242|Staircase Sandstone Member|42249|6|Mentioned|p21|||||||||
17242|Staircase Sandstone Member|42578|6|Mentioned|Table 1 P124-125|||Actually spelt Staircase Ss Mb.||||||
17242|Staircase Sandstone Member|42856|5|Briefly described|p639|||||||||
17242|Staircase Sandstone Member|42974|5|Briefly described|p202|||of Cattle Creek Formation||||||
17242|Staircase Sandstone Member|43050|5|Briefly described|p18|||of Cattle Creek Formation||||||
17242|Staircase Sandstone Member|44172|4|Described|p1320,1327-8,1331,||Artinskian|p1336,Fig..2,Tb.1||||||
17242|Staircase Sandstone Member|44173|14|Not recorded|p109-111||Early Permian|Member of Cattle Creek Formation.||||||
17242|Staircase Sandstone Member|45071|3|Fully described|Table 6|||||||||
17242|Staircase Sandstone Member|46849|6|Mentioned|Fig. 7|||||||||
17242|Staircase Sandstone Member|60286|5|Briefly described|p298 Fig.11|Early Permian|Early Permian|Of Cattle Creek Formation. Overlies Moorooloo Mudstone Member. Contains Cruziana and Skolithos trace fossil assemblage. Geological Province: Bowen Basin.||||||
17242|Staircase Sandstone Member|68576|5|Briefly described|Q_4: p7-8, p19, p24|Cisuralian|Cisuralian|Bowen Basin. Appears as Staircase Sandstone on p7 and p24. Fossil shells occur in the uppermost few metres.||Cattle Creek Formation.||Is overlain by Sirius Mudstone Member.|Light grey, fine to very coarse and pebbly, mostly medium, fairly and poorly sorted, sub-labile to labile with a mostly argillaceous matrix, in part siliceous and calcareous. Plant fragments, shale casts, scattered quartz pebbles throughout.|
17256|Stanbroke Sandstone|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17256|Stanbroke Sandstone|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17256|Stanbroke Sandstone|37862|4|Described|p583|||||||||
17256|Stanbroke Sandstone|38310|6|Mentioned|p237|||||||||
17256|Stanbroke Sandstone|38350|4|Described|p11|||||||||
17256|Stanbroke Sandstone|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17256|Stanbroke Sandstone|39445|5|Briefly described|Table 2|||||||||
17256|Stanbroke Sandstone|40840|6|Mentioned|Map legend|||||||||
17256|Stanbroke Sandstone|42565|5|Briefly described|Table 1 P5|||||||||
17256|Stanbroke Sandstone|45161|4|Described|p26|||||||||
17256|Stanbroke Sandstone|45166|5|Briefly described|p17|||||||||
17256|Stanbroke Sandstone|46960|6|Mentioned|p216|||||||||
17256|Stanbroke Sandstone|46962|4|Described|Table 1|||See also Fig.3.||||||
17256|Stanbroke Sandstone|46996|6|Mentioned|p273|||||||||
17256|Stanbroke Sandstone|49009|2|Defined|p43|Proterozoic|Proterozoic|Previously mapped as part of the Argylla Formation (Carter and Opik 63).||||||02-APR-07
17256|Stanbroke Sandstone|49041|5|Briefly described|Table 1|||||||||
17256|Stanbroke Sandstone|50100|5|Briefly described|p13 Fig. 4, p19|Statherian|Statherian|Mainly quartzose to feldspathic sst., with local basal conglomerates containing volcanic detritus; includes some calcareous and dolomitic beds; extensively recrystallised.  Overlies Magna Lynn Metabasalt and Argylla Fm.  Geol.Prov: Kalkadoon-Ewen Prov.||||||04-DEC-06
17256|Stanbroke Sandstone|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite, dolomite, limestone, siltstone, basal conglomerate.||||||
17256|Stanbroke Sandstone|64250|6|Mentioned|p8|||Omitted from stratigraphic chart because of limited exposure.||||||
17256|Stanbroke Sandstone|65396|6|Mentioned|p174|||Southern Kalkadoon-Leichhardt Belt. Small unit with limited exposure.||||(Possibly) Correlated with Ballara Quartzite.||
17256|Stanbroke Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p107|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Kalkadoon-Leichhardt Domain, Mount Isa Inlier. Calvert Superbasin.|||||Quartz arenite, feldspathic arenite, calcareous arenite, limestone, greywacke, siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|69591|5|Briefly described|p38 Fig.2.22, p39-40, p55|||Kalkadoon-Leichhardt Domain, Calvert Superbasin. Age uncertain; considered part of the Prize and Gun Supersequences.|||||Quartz arenite, feldspathic arenite, calcareous arenite, limestone, greywacke, siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Broad age range. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Shown as younger than the Argylla Formation.||||Shown as laterally equivalent to Mary Kathleen Group, Quilalar Formation.|Quartzose to feldspathic sandstone, calcareous sandstone, limestone, lithic sandstoneand siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Kalkadoon-Leichhardt Domain. Broad age range. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma). Shown as younger than the Argylla Formation.||||Shown as laterally equivalent to the Mary Kathleen Group, Quilalar Formation.|Quartzose to feldspathic sandstone, calcareous sandstone, limestone, lithic sandstoneand siltstone, local basal conglomerate.|
17256|Stanbroke Sandstone|73525|6|Mentioned|p4-5 Fig.2|||Kalkadoon-Leichhardt Domain.|||||Clastics.|
17264|Stanleigh Formation|30340|6|Mentioned|Table 3|||||||||
17264|Stanleigh Formation|30341|6|Mentioned|p136|||Lower Permian age||||||
17264|Stanleigh Formation|30450|6|Mentioned|Table 1|||Permian age. Southwest Bowen Basin||||||
17264|Stanleigh Formation|30545|6|Mentioned|Fig.2|||Artinskian. See also p22||||||25-FEB-22
17264|Stanleigh Formation|30546|6|Mentioned|p107|||Correlation||||||
17264|Stanleigh Formation|30914|6|Mentioned|Map legend|Permian|Permian|||||||
17264|Stanleigh Formation|31120|6|Mentioned|p147|||Refers Mollan et al. (1969)||||||
17264|Stanleigh Formation|31396|6|Mentioned|p1185|||||||||
17264|Stanleigh Formation|32577|6|Mentioned|p23|||||||||
17264|Stanleigh Formation|32840|6|Mentioned|p11|||||||||
17264|Stanleigh Formation|33701|6|Mentioned|Fig.1|||Artinskian.||||||
17264|Stanleigh Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
17264|Stanleigh Formation|34390|4|Described|Table 2|||Permian||||||
17264|Stanleigh Formation|34392|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
17264|Stanleigh Formation|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
17264|Stanleigh Formation|37726|6|Mentioned|Fig.2|||||||||
17264|Stanleigh Formation|38444|6|Mentioned|p302|||||||||
17264|Stanleigh Formation|39212|6|Mentioned|p11|||||||||
17264|Stanleigh Formation|39220|6|Mentioned|p42|||Oldest Perm. Marine fossils||||||
17264|Stanleigh Formation|39445|5|Briefly described|p104, Table 8 p110|||||||||25-FEB-22
17264|Stanleigh Formation|41639|6|Mentioned|p7|||||||||
17264|Stanleigh Formation|42614|5|Briefly described|p13|||Bowen Basin||||||
17264|Stanleigh Formation|42994|6|Mentioned|p266|||||||||
17264|Stanleigh Formation|43471|14|Not recorded|p229,238,239|||Megadesmus, Astartila||||||
17264|Stanleigh Formation|43474|14|Not recorded|p7,46,72||Artinskian|||||||
17264|Stanleigh Formation|43987|14|Not recorded|p266,270|||||||||
17264|Stanleigh Formation|43990|14|Not recorded|Map Legend|||Part of Tiverton Sub-Group.||||||
17264|Stanleigh Formation|43994|14|Not recorded|Map Legend|||||||||
17264|Stanleigh Formation|44000|14|Not recorded|p32|||||||||
17264|Stanleigh Formation|44115|14|Not recorded|p19|||||||||
17264|Stanleigh Formation|44172|14|Not recorded|Tb.1,p1325,1331||Late Permian|Ref. to Laing 1961 (unpubl.)||||||
17264|Stanleigh Formation|44173|14|Not recorded|p109-111,113|||||||||
17264|Stanleigh Formation|44218|14|Not recorded|p19||Sakmarian|late Sakmarian||||||
17264|Stanleigh Formation|44219|14|Not recorded|p31,32||Artinskian|||||||
17264|Stanleigh Formation|44337|5|Briefly described|Map Legend|Late Permian|Early Permian|Lithology.||||||
17264|Stanleigh Formation|44422|14|Not recorded|p151||Early Permian|May be equivalent to lower part of Cattle Creek Formation.||||||
17264|Stanleigh Formation|44424|14|Not recorded|p293-301|||In Tiverton Subgroup.||||||
17264|Stanleigh Formation|44426|14|Not recorded|p11|||||||||
17264|Stanleigh Formation|44489|14|Not recorded|p68,70|||||||||
17264|Stanleigh Formation|45006|14|Not recorded|p80|||||||||
17264|Stanleigh Formation|45031|14|Not recorded|p9-11,Fig.3||Permian|||||||
17264|Stanleigh Formation|45071|3|Fully described|Table 6|||||||||
17264|Stanleigh Formation|48630|14|Not recorded|p1,4,5,7,13,18,20,22|||Pls.1,2||||||
17264|Stanleigh Formation|48900|3|Fully described|p28|||Lower Permian||||||
17264|Stanleigh Formation|49644|5|Briefly described|Table|||||||||
17274|Stanthorpe Granite|33437|6|Mentioned|Fig.1|||U.Perm.||||||
17274|Stanthorpe Granite|34423|6|Mentioned|p293|||On Table.||||||
17274|Stanthorpe Granite|34479|6|Mentioned|p312|||Permian ?||||||
17274|Stanthorpe Granite|34589|6|Mentioned|p275|||225 my||||||
17274|Stanthorpe Granite|36045|6|Mentioned|Fig.7|||||||||
17274|Stanthorpe Granite|39838|5|Briefly described|p341|||||||||
17274|Stanthorpe Granite|42559|4|Described|p13|||||||||
17274|Stanthorpe Granite|44068|14|Not recorded|p13|||||||||
17274|Stanthorpe Granite|44512|14|Not recorded|p16,17,map|||Intrudes "Silverwood Group". (epi-Permian or early Triassic)||||||
17274|Stanthorpe Granite|44563|14|Not recorded|p142-143|||||||||
17274|Stanthorpe Granite|44564|14|Not recorded|p166|||||||||
17274|Stanthorpe Granite|44625|14|Not recorded|p383,384|||||||||
17274|Stanthorpe Granite|44671|4|Described|p245|||||||||
17274|Stanthorpe Granite|44832|14|Not recorded|p9,10,13|||||||||
17274|Stanthorpe Granite|45087|5|Briefly described|p16|||Chemical analyses||||||
17274|Stanthorpe Granite|61772|6|Mentioned|p131|Triassic|Permian|||||||
17274|Stanthorpe Granite|63731|5|Briefly described|Map legend|Early Triassic|Early Triassic|Detailed lithology presented.||||||
17274|Stanthorpe Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Monzogranite to syenogranite.||||||
17274|Stanthorpe Granite|63748|3|Fully described|p36-39, p86 Appdx. 1|Early Triassic|Permian|Two outcroppings are referred to informally as Mayland River complex (NE) and Stanthorpe complex (in SW Stanthorpe-Wallangarra region). Age: 246.9+/-2.0Ma (U-Pb zircon SHRIMP). Intrudes Texas beds. I-type. Detailed lithology.See also p16, p25, p27 Fig. 27||||||07-FEB-11
17274|Stanthorpe Granite|65668|6|Mentioned|p32|Permian|Permian|Intrudes the Wallangarra Volcanics. Age ~247 Ma.||||||
17274|Stanthorpe Granite|67818|5|Briefly described|p131, Fig. 2|Middle Triassic|Middle Triassic|Northern New England region. Rb/Sr biotite age (Shaw, 1994), U/Pb zircon SHRIMP age (Hughes, 1993).|240.2 Ma Rb/Sr, ~237 Ma U/Pb|||||03-OCT-14
17274|Stanthorpe Granite|68111|5|Briefly described|p969 Tb.1|Anisian|Olenekian|Mis-spelt as Stanthrope. Also 243 - 238 Ma, Rb-Sr (biotite) (Shaw 1994).|246.9 +/- 2.0 Ma; U-Pb SHRIMP(Donchak et al 2007)|Of the Stanthorpe Supersuite.||||
17274|Stanthorpe Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Sailor Jack and Dormans Flat Granites, are all mapped under the symbol, Rgn.||||||
17274|Stanthorpe Granite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
17274|Stanthorpe Granite|68679|4|Described|p446, p453-458, p461-466|Middle Triassic|Middle Triassic|By far the most extensive unit in the New England Batholith. ~1840 km2. Geochemistry discussed in some detail; geochemical plots, photographs. I-type. Similarities with Ruby Creek Granite. Associated with minor Mo mineralisation. Has untapped potential for dimension stone.|246.9 +/- 2.0 Ma (SHRIMP U-Pb zircon: GA).|Stanthorpe Suite.||Intrudes the Wallangarra Volcanics, Bungulla Monzogranite, Palgrave, Ballandean Granites. Is intruded by Ruby Creek Granite.|Pink, white or brown, medium-grained, porphyritic, leucocratic biotite monzogranite to syenogranite; minor hornblende-biotite monzogranite, aplitic leucogranite; local rapakivi textures, granophyric, miarolitic, vuggy pegmatite/aplo-pegmatite lenses.|
17274|Stanthorpe Granite|68901|5|Briefly described|p8, p128,129, 132,134, 136, 137|Early Triassic|Early Triassic|Rb-Sr ages: 238.1 - 242.2 Ma (Shaw, 1994). Close genetic relationship with Ruby Creek granite supported.|246.9+/-2 Ma SHRIMP, Donchak et al., 2007.|||Intrudes the Ballandean Granite. Intruded by the Ruby Creek Granite.||27-SEP-18
17274|Stanthorpe Granite|69639|4|Described|p2, p6, p8, p80, p151, p157|Triassic|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. See also  p163-p168, p192-p193, p222, p239.|248.7 +/- 1.2 Ma (SHRIMP U-Pb)|Stanthorpe Suite||Intrudes and is faulted against the Maryland Granite. Faulted against the Koreelan Creek Granodiorite. Intrudes the Bookookoorara Monzogranite.|Massive, coarse-grained, alkali  feldspar-rich leucocratic granite (syenogranite).|
17274|Stanthorpe Granite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
17274|Stanthorpe Granite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Olenekian|New England Orogen. A SHRIMP age derived from unpublished Geoscience Australia data of 246.9 +/- 2.0 Ma is also provided.|248.7 +/- 1.2 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
17274|Stanthorpe Granite|70373|6|Mentioned|p800|Triassic|Triassic|May show fault displacement.|~250 Ma|||||
17274|Stanthorpe Granite|70876|5|Briefly described|p80|||Mineralisation is mentioned but no details are provided.||Stanthorpe Supersuite||||
17274|Stanthorpe Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|249+/-1.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
17274|Stanthorpe Granite|71628|6|Mentioned|p15: 32, 38, 40, 81|||Gradwell (1960), after the ""Stanthorpe"" granite of Saint-Smith (1913, 1914). Now Stanthorpe Complex.||||||
17274|Stanthorpe Granite|72078|6|Mentioned|p4|||Geological province: New England Orogen. Together with the Ruby Creek Leucogranite forms the Ruby Creek Sn-W district.||||||14-JAN-20
17274|Stanthorpe Granite|72297|6|Mentioned|p759|||Gem-quality colourless (rarely blue) topaz with rare garnet and zircon occur in alluvium and tailings from tin mining near Stanthorpe; derived from cassiterite-bearing veins and greisen zones in the granite.||||||
17277|Stanthorpe Suite|38839|6|Mentioned|p244|||Geological Province: New England Fold Belt.||||||12-AUG-08
17277|Stanthorpe Suite|42876|6|Mentioned|Fig.1, p142|||Variation on Stanthorpe Granite, Adamellite?||||||
17277|Stanthorpe Suite|42997|6|Mentioned|Fig.2,p37|||||||||
17277|Stanthorpe Suite|63748|5|Briefly described|p36-37|Early Triassic|Permian|Of the Stanthorpe Supersuite. Includes Stanthorpe and Ruby Creek Granites.||||||07-FEB-11
17277|Stanthorpe Suite|68679|5|Briefly described|p456, p458-464, p466|||Northern New England Batholith. Placed into the Moonbi Supersuite by Blevin and Chappell (1996) and Bryant and Chappell (2010). Geochemistry discussed. Historical reports of high Au values in the Pikedale lode.|~248-245 Ma.|Stanthorpe Supersuite.|Ruby Creek, Stanthorpe Granites.|||
17277|Stanthorpe Suite|69639|5|Briefly described|p9, p26, p163, p175, p181, p187|||New England Orogen.||Stanthorpe Supersuite|Includes the Stanthorpe Granite, Morgans Creek Monzogranite, Ruby Creek Granite and the Rivertree Granite.|||
17277|Stanthorpe Suite|71628|5|Briefly described|p11: 5, 35, 46-47, 53, 58, 73, 77, 98|||See also p16-26; p17: 15, 20, 25, 31, 33, 38, 43, 56, 58, 62, 66, 69, 88, 93, 95, 99; p19: 20, 131, 175. Korsch (1977).||Stanthorpe Supersuite.||||
17284|Stanwell Coal Measures|24571|6|Mentioned|p13|||||||||
17284|Stanwell Coal Measures|24615|5|Briefly described|CD|Cretaceous|Cretaceous|[Ks].  Mudstone, sandstone, siltstone, minor coal.||||||
17284|Stanwell Coal Measures|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
17284|Stanwell Coal Measures|31086|6|Mentioned|p37|||||||||
17284|Stanwell Coal Measures|31657|4|Described|p96|||Neocomian to Aptian or Albian||||||
17284|Stanwell Coal Measures|31658|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17284|Stanwell Coal Measures|31659|4|Described|p75|Cretaceous|Cretaceous|Mudstone, sandstone, claystone, coal. See also Table 1.||||||08-OCT-08
17284|Stanwell Coal Measures|32358|4|Described|Table 3|||P16||||||
17284|Stanwell Coal Measures|33165|6|Mentioned|Chart|||Correlation chart only||||||
17284|Stanwell Coal Measures|33879|6|Mentioned|p287|||||||||
17284|Stanwell Coal Measures|35053|5|Briefly described|p38|||||||||
17284|Stanwell Coal Measures|35069|6|Mentioned|Fig.1|||||||||
17284|Stanwell Coal Measures|35266|6|Mentioned|p202|||||||||
17284|Stanwell Coal Measures|35952|5|Briefly described|p500|||Regional geology.||||||
17284|Stanwell Coal Measures|36581|6|Mentioned|p464|||||||||
17284|Stanwell Coal Measures|37565|6|Mentioned|p10|||||||||
17284|Stanwell Coal Measures|37860|6|Mentioned|p571|||||||||
17284|Stanwell Coal Measures|38081|5|Briefly described|Table 1|||||||||
17284|Stanwell Coal Measures|38084|5|Briefly described|p56|||||||||
17284|Stanwell Coal Measures|38153|6|Mentioned|p375|||||||||
17284|Stanwell Coal Measures|38406|6|Mentioned|p12|||||||||
17284|Stanwell Coal Measures|39211|5|Briefly described|p43|||||||||
17284|Stanwell Coal Measures|39445|5|Briefly described|Table 11|||||||||
17284|Stanwell Coal Measures|41057|6|Mentioned|p62|||||||||
17284|Stanwell Coal Measures|41246|6|Mentioned|Map legend|Cretaceous||||||||
17284|Stanwell Coal Measures|41576|4|Described|p19|||See also Table 1||||||
17284|Stanwell Coal Measures|41577|6|Mentioned|Map legend|Early Cretaceous||||||||
17284|Stanwell Coal Measures|41922|4|Described|Table 1, P8|||||||||
17284|Stanwell Coal Measures|41931|6|Mentioned|p96|||||||||
17284|Stanwell Coal Measures|44029|14|Not recorded|p158||Late Jurassic|||||||
17284|Stanwell Coal Measures|44082|6|Mentioned|p28,Tb.34|Albian|Aptian|(Aptian-Early Albian) Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
17284|Stanwell Coal Measures|44084|14|Not recorded|p2,10,14,16|||||||||
17284|Stanwell Coal Measures|44091|14|Not recorded|p61||Cretaceous|||||||
17284|Stanwell Coal Measures|44128|14|Not recorded|Tb.1,p426|||||||||
17284|Stanwell Coal Measures|44360|14|Not recorded|p36||Neocomian|See also Lexicon.||||||
17284|Stanwell Coal Measures|44369|14|Not recorded|p173,Fig.23|||||||||
17284|Stanwell Coal Measures|44377|14|Not recorded|p15|Neocomian|Late Jurassic|See also Lexicon.||||||
17284|Stanwell Coal Measures|44742|14|Not recorded|p82-84,92||Early Cretaceous|||||||
17284|Stanwell Coal Measures|44997|14|Not recorded|p.21|||||||||
17284|Stanwell Coal Measures|50209|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||||||
17284|Stanwell Coal Measures|50317|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Mudstone, sandstone, siltstone, minor coal.||||||09-JUN-04
17284|Stanwell Coal Measures|60557|5|Briefly described|p19 Fig. 5b, p28|Early Cretaceous|Early Cretaceous|||||||
17284|Stanwell Coal Measures|68008|5|Briefly described|p243, p261, p264|Early Cretaceous|Early Cretaceous|First named by Dunstan (1912), after work by Rands (1892), Jack and Etheridge (1892), Maitland (1895) and Dunstan (1898). Regarded as correlative of Ipswich Coal Measures, and included part of the Precipice Sandstone. Later correlated with the Walloon Series by Walkom (1915, 1917). Only one occurrence of coal (Helby and Paltridge, 1977) has been found in this unit despite over a century of exploration, so its name is changed in this study to Stanwell Formation (Murray et al., 2012).||||||
17284|Stanwell Coal Measures|69594|5|Briefly described|p550-552|Albian|Albian|Dunstan (1898). Stanwell Basin. At least 215m thick. Revised by Murray (2007) and Murray et al. (2012) as Razorback beds (Precipice Sandstone) for the upper part, and the lower, marginal marine succession was named the Stanwell Formation. Previous errors of age range discussed, including correlation with Walloon Series.||||Correlated with Styx Coal Measures and (partly) Jim Crow beds.|Basal marine sandstone, overlain by non-marine sediments.|
17296|Star of Hope Formation|22540|6|Mentioned|Fig.1 p778|Visean|Visean|||||||
17296|Star of Hope Formation|22675|3|Fully described|p35|Early Carboniferous|Early Carboniferous|Drummond Basin.||||||21-OCT-08
17296|Star of Hope Formation|23052|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
17296|Star of Hope Formation|23082|6|Mentioned|p686|||||||||
17296|Star of Hope Formation|23161|4|Described|p14 table2b|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|23184|6|Mentioned|Fig1p178|Arundian|Chadian|||||||
17296|Star of Hope Formation|23430|5|Briefly described|p510|||Drummond Basin Province||||||
17296|Star of Hope Formation|23504|5|Briefly described|Map Legend||Carboniferous|||||||
17296|Star of Hope Formation|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V74.||||||
17296|Star of Hope Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Early Carboniferous|Varicoloured tuff and tuffaceous sandstone;  minor conglomerate, siltstone and mudstone.  Max. thickness: 1000m.  Geological Province: Drummond Basin.||||||18-JAN-06
17296|Star of Hope Formation|24424|5|Briefly described|p539 Tb.4|Namurian|Middle Devonian|Age: 320-370 Ma. Palaeomagnetic poles given.||||||04-FEB-05
17296|Star of Hope Formation|30151|6|Mentioned|p13|||Upper Devonian? - Lower Carboniferous. See also Fig.3.||||||
17296|Star of Hope Formation|30691|4|Described|p13|||Lower Carboniferous age. See also Table 3. Of Drummond Group.||||||21-OCT-08
17296|Star of Hope Formation|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|Devonian - Carboniferous||||||
17296|Star of Hope Formation|31984|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|32490|4|Described|Table 1|||L.Carb.||||||
17296|Star of Hope Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|32553|4|Described|p46|||||||||
17296|Star of Hope Formation|32556|4|Described|Table 2|||L.Carb.||||||
17296|Star of Hope Formation|32639|6|Mentioned|p76|||||||||
17296|Star of Hope Formation|33086|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|33092|5|Briefly described|p7|||Stratigraphic table||||||
17296|Star of Hope Formation|33096|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|33645|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17296|Star of Hope Formation|33646|6|Mentioned|p18|||||||||
17296|Star of Hope Formation|34174|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|34389|4|Described|Table 1|||Lower Carboniferous||||||
17296|Star of Hope Formation|34390|4|Described|Table 1|||Lower Carboniferous.||||||21-OCT-08
17296|Star of Hope Formation|34391|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|34392|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|34408|6|Mentioned|p185|||On table||||||
17296|Star of Hope Formation|34409|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|35811|5|Briefly described|Table 4|||||||||
17296|Star of Hope Formation|36472|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17296|Star of Hope Formation|37451|6|Mentioned|Table 2|||||||||
17296|Star of Hope Formation|37573|4|Described|Table 2|||||||||
17296|Star of Hope Formation|37613|6|Mentioned|p249|||See also Fig.3||||||
17296|Star of Hope Formation|38666|6|Mentioned|p4|||||||||
17296|Star of Hope Formation|39445|5|Briefly described|Table 6|||||||||
17296|Star of Hope Formation|41120|6|Mentioned|p193|||||||||
17296|Star of Hope Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
17296|Star of Hope Formation|41272|5|Briefly described|M 1of1 M10|||||||||
17296|Star of Hope Formation|41710|5|Briefly described|p226|||||||||
17296|Star of Hope Formation|41805|5|Briefly described|p26|||||||||
17296|Star of Hope Formation|42486|5|Briefly described|p201|||||||||
17296|Star of Hope Formation|42547|5|Briefly described|p61|||||||||
17296|Star of Hope Formation|42614|5|Briefly described|Table 1 P5|||||||||
17296|Star of Hope Formation|42633|4|Described|p19|||||||||
17296|Star of Hope Formation|42701|4|Described|p27|||||||||
17296|Star of Hope Formation|43105|5|Briefly described|p12|||||||||
17296|Star of Hope Formation|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||underlies Ducabrook Formation; overlies Raymond Sandstone||23-DEC-11
17296|Star of Hope Formation|43213|4|Described|p85-86, p92, p94, p238|||Of de Bretizel (1966), who applied the name to the lower part of Hill's (1957) Ducabrook Formation. Red Mountain and Eastern Creek areas. Fluviatile and lacustrine sediments from a coeval volcanic arc to the east. Geophysics described.||||Overlies Raymond Formation. Disconformably overlies Silver Hills Volcanics. Is overlain conformably by Ducabrook Formation.|Quartz-pebble conglomerate; volcanilithic sandstone, tuff and interbedded quartz-pebble conglomerate.|
17296|Star of Hope Formation|43259|4|Described|Appendix 1,p7.||Early Carboniferous|||||||
17296|Star of Hope Formation|43391|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Geological Province: Drummond Basin.  Includes a series of four unnamed volcanic members.||||||23-JUN-04
17296|Star of Hope Formation|43706|5|Briefly described|p12|Early Carboniferous|Early Carboniferous|(Early Carb.- Middle Carb.)||||||
17296|Star of Hope Formation|43727|6|Mentioned|p1|||||||||
17296|Star of Hope Formation|43934|5|Briefly described|Map Legend||Carboniferous|||||||
17296|Star of Hope Formation|43936|5|Briefly described|Map Legend||Carboniferous|||||||
17296|Star of Hope Formation|44081|14|Not recorded|p79,85-9,91,102,139,|||Fig.7,185,196,Pl.8||||||
17296|Star of Hope Formation|44245|5|Briefly described|Map Legend||Carboniferous|||||||
17296|Star of Hope Formation|44331|14|Not recorded|Map Legend||Early Carboniferous|||||||
17296|Star of Hope Formation|45073|3|Fully described|p39|||Refers de Bretizel (1966).||||||21-OCT-08
17296|Star of Hope Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
17296|Star of Hope Formation|45151|5|Briefly described|Table 6|||||||||
17296|Star of Hope Formation|46849|6|Mentioned|Fig. 2|||||||||
17296|Star of Hope Formation|46881|6|Mentioned|Table 2|||||||||
17296|Star of Hope Formation|48914|6|Mentioned|p35|||L.Carb.||||||
17296|Star of Hope Formation|48920|3|Fully described|p20|||Lower Carboniferous. Part of Drummond Group.||||||21-OCT-08
17296|Star of Hope Formation|48922|4|Described|p12|||||||||
17296|Star of Hope Formation|48951|6|Mentioned|Table 1|||||||||
17296|Star of Hope Formation|50153|6|Mentioned|p17|||||||||
17296|Star of Hope Formation|60659|4|Described|p14, p50 Fig. 2|Early Carboniferous|Early Carboniferous|Transgressive and overlies Raymond Formation, and Scartwater Formation. Conformably overlain by by Bulliwallah Formation. Geological Province: Drummond Basin.||||||07-FEB-11
17296|Star of Hope Formation|61394|5|Briefly described|p964 Fig. 1|Visean|Visean|Geological Province: southern Drummond Basin.||||||
17296|Star of Hope Formation|64315|5|Briefly described|p510 Tb. 1|Early Carboniferous|Early Carboniferous|Max. thickness: 1000m. Geological province: southern Drummond Basin. Varicoloured tuff, tuffaceous sandstone; minor conglomerate, siltstone, mudstone.||||||
17296|Star of Hope Formation|64849|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.||||||
17296|Star of Hope Formation|64850|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.||||||09-FEB-09
17296|Star of Hope Formation|64851|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.||||||
17296|Star of Hope Formation|64852|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.||||||
17296|Star of Hope Formation|66085|5|Briefly described|Map legend|Carboniferous|Carboniferous|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.||||||
17296|Star of Hope Formation|66188|6|Mentioned|Fig 3, TB1, Fig 16-17|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
17296|Star of Hope Formation|67402|4|Described|p165 tbl LPB1, p196 fig DRM2|Visean|Visean|Drummond Basin. Deposited in a low-energy fluvial environment. Approximately 900m thick. See also p197, p198 fig DRM3, p200 fig DRM6/DRM7, p201, p202, p203 fig DRM11.||||Overlies the Raymond and Mount Hall Formations. Overlain by the Bulliwallah Formation and Ducabrook Formation.|Pebbly quartz sandstone, arkosic sandstone, quartz-pebble conglomerate, volcano-lithic sandstone, siltstone; some mudstone, tuff, rhyolite and sinter.|
17296|Star of Hope Formation|68326|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drumond Basin.||||Conformably overlies Raymond Sandstone. Is overlain conformably by Ducabrook Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|02-DEC-13
17296|Star of Hope Formation|68328|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Conformably overlies Raymond Sandstone. Is intruded by Withersfield Granite. Is overlain conformably by Ducabrook Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68329|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|||||Conformably overlies Mount Hall Formation. Is overlain conformably by Bulliwallah Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68347|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Mount Hall Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68404|5|Briefly described|Map legend|Carboniferous|Carboniferous|Drummond Basin|||||Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|17-JUN-13
17296|Star of Hope Formation|68411|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin||||Conformably overlain by the Ducabrook Formation. Conformably underlain by the Raymond Sandstone or Mount Hall Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolite to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68412|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlies Raymond Sandstone. Is conformably overlain by Ducabrook Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|23-JUN-15
17296|Star of Hope Formation|68413|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||Conformably underlain by the Raymond Sandstone. Conformably overlain by the Bulliwallah Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68414|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin. Map symbol (Cs) indicates Carboniferous age.||||Conformably overlain by the Ducabrook Formation. Conformably underlain by the Mount Hall Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|29-AUG-14
17296|Star of Hope Formation|68423|5|Briefly described|map legend|Early Carboniferous|Early Carboniferous|Drummond Basin. This unit is incorrectly colour-coded in the "Palaeozoic Units" inset on the sheet.||||Conformably overlies Raymond Sandstone. Is overlain conformably by Ducabrook Formation.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68482|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlain by the Ducabrook Formation. Conformably underlain by the Raymond Sandstone.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Bulliwallah, Ducabrook, Mount Rankin and Natal Formations, are all mapped under the symbol, Cd3.||||||
17296|Star of Hope Formation|68679|6|Mentioned|p364|Carboniferous|Carboniferous|Thomson Orogen.||||||
17296|Star of Hope Formation|68731|5|Briefly described|p191 Fig 3.102, p196|Mississippian|Mississippian|Distributed throughout the eastern segment of the Drummond Basin. < 1800 m thick. Detailed lithology discussed. Macroflora indicates Mississippian (White cited in Olgers 1972).||||Conformably overlain by the Ducabrook Formation. Conformably overlain by the Bulliwallah Formation.|Comprises predominantly volcanilithic siltstone and sandstone with minor conglomerate, ignimbrite and accretionary lapilli tuff.|18-JUL-14
17296|Star of Hope Formation|68900|2|Defined|p4, p37, p64, p66-p72|Carboniferous|Carboniferous|Drummond Basin. Originally named by de Bretizel (1966) for the units between the Raymond and Ducabrook formations. The type area is in the Star of Hope Syncline in ALBRO. This unit generally produces low hills and commonly displays bedding trends on airphotos. This unit has a slightly enriched radiometric signature, particularly in K bands. The unit has a very low response in airborne magnetic images. Lithology and fossil assemblage is discussed in detail. Volcanic and volcaniclastic rocks deposited in a subaerial environment whilst the sedimentary rocks are interpreted to have been deposited in a fluvial setting. Thickness is variable between 150m to 600m in the southern Drummond Basin, around 950m thick in NATAL DOWNS and at least 1800m in HARVEST HOME.||||Conformably overlies the Mount Hall Formation and the Raymond Formation. Overlies the Scartwater Formation. Conformably overlain by the Bulliwallah Formation and Ducabrook Formation.|Dominantly volcanolithic sedimentary rocks, particularly siltstone and sandstone. Rare rock types include conglomerate as well as primary volcanic rocks such as ignimbrite and accretionary lapilli tuff.|
17296|Star of Hope Formation|68901|6|Mentioned|p2 Fig. i|Carboniferous|Carboniferous|||||||27-SEP-18
17296|Star of Hope Formation|69379|5|Briefly described|map legend|Early Carboniferous|Late Devonian||||||Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter|
17296|Star of Hope Formation|69952|6|Mentioned|p85|Carboniferous|Carboniferous|Thomson Orogen.||||||
17296|Star of Hope Formation|70740|5|Briefly described|p2, p7, p9, p76-p77|Early Carboniferous|Early Carboniferous|Drummond Basin. Age based on rich plant fossil assemblage. See also  p80, p87, p103, p105-p106, p123-p124.||||Overlies the Scartwater Formation, underlies the Arundel Rhyolite. Overlies the Stones Creek Volcanics and the Saint Anns Formation. Intruded by Glen Easter Leucogranite.|Volcanolithic siltstone and sandstone, conglomerate, rhyolitic ignimbrite and accretionary lapilli tuff.|
17296|Star of Hope Formation|70856|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||Overlain conformably by Ducabrook Formation, overlies Mount Hall Formation conformably.|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|70857|5|Briefly described|Map Legend|Carboniferous|Devonian|||||Overlain by Ducabrook Formation, overlies Mount Hall Formation|Lithic conglomerate, feldspatholithic sandstone, rhyolitic to dacitic ignimbrite and flows, tuffaceous siltstone and rare sinter.|
17296|Star of Hope Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Early Carboniferous|Geological province: Drummond Basin.||||Overlain by Bulliwallah Formation and Ducabrook Formation in the northern and southern Drummond Basin respectively. Underlain by Raymond Formation.||
17296|Star of Hope Formation|73198|4|Described|p499-502, p504-507, p509-511, p513-516|||[Written as Star o Hope Formation; probably misspelt]. Drummond Basin. Originally part of Cycle 3 of Olgers (1972); combined with Cycle 2 herein. Maximum thickness: 1800 m in the north [thinning rapidly towards the basin margins] (thickest interval observed in this study is 378 m). Red-purple colour of strata [was previously] interpreted to reflect a volcanic influence. Variable clast composition in northern and southern parts of the basin. Coarse-grained rocks are indistinguishable from the Mt Hall Formation, other than by stratigraphic position, but sandstones are less quartzose. Volcanic influence is sparse to virtually absent. Top shows a fining-upward trend. Contact with overlying Bulliwallah Formation is erosional but probably conformable. Compositionally overlaps with [previous] Cycle 2.  Variably orientated paleocurrent indicators in the central part of the basin. Basement provenance. [See article for petrographic descriptions and data].||||Underlain by Raymond Formation. Conformably overlain by Ducabrook Formation and Bulliwallah Formation.|Distinctly red-purple quartz to feldspathic sandstone and pebble conglomerate, volcanolithic sandstone, mudstone and silicic tuff.|
17306|Staveley Formation|22460|5|Briefly described|p447|||Of the Mary Kathleen Group.||||||02-APR-07
17306|Staveley Formation|22461|4|Described|p475-476.|||Also see p463 and Fig 1 p464. Overlain by Marimo Slate.||||||02-APR-07
17306|Staveley Formation|22667|6|Mentioned|P235|||||||||
17306|Staveley Formation|22720|5|Briefly described|p 167|||||||||
17306|Staveley Formation|22747|6|Mentioned|Table1,p7|||Correlates with Corella Formation||||||
17306|Staveley Formation|23064|4|Described|135|||Geological province: Mt Isa Inlier. Of the Mary Kathleen Group.||||||02-APR-07
17306|Staveley Formation|23068|5|Briefly described|p784 (fig 1)|||||||||
17306|Staveley Formation|23069|5|Briefly described|p775 (fig 1)|||||||||
17306|Staveley Formation|23070|4|Described|p769 (fig 1)|||||||||
17306|Staveley Formation|23333|4|Described|1114 Fig.1|Statherian|Statherian|||||||
17306|Staveley Formation|23471|5|Briefly described|p111|||Of Mary Kathleen Group. Geological Province: Mount Isa Block.||||||
17306|Staveley Formation|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.  Of the Mary Kathleen Group.||||||02-APR-07
17306|Staveley Formation|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Mary Kathleen Group||||||
17306|Staveley Formation|23973|5|Briefly described|p1435|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Mary Kathleen Group.||||||29-APR-16
17306|Staveley Formation|23974|5|Briefly described|p1450|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
17306|Staveley Formation|23975|5|Briefly described|p1464|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Mary Kathleen Group.||||||
17306|Staveley Formation|29969|6|Mentioned|Table 1|||||||||
17306|Staveley Formation|30531|6|Mentioned|p15|||Also Mention P17 and P22||||||
17306|Staveley Formation|33900|6|Mentioned|p15|||See also P18.||||||
17306|Staveley Formation|35074|6|Mentioned|Fig.2|||||||||
17306|Staveley Formation|37862|4|Described|p588|||||||||
17306|Staveley Formation|38234|4|Described|p104|||||||||
17306|Staveley Formation|38235|6|Mentioned|p116|||||||||
17306|Staveley Formation|38833|6|Mentioned|p161|||||||||
17306|Staveley Formation|38834|6|Mentioned|p163|||||||||
17306|Staveley Formation|39029|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
17306|Staveley Formation|39043|6|Mentioned|p9|||||||||
17306|Staveley Formation|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17306|Staveley Formation|39445|5|Briefly described|Table 2|||See also p43.||||||02-APR-07
17306|Staveley Formation|39496|4|Described|p12|||||||||
17306|Staveley Formation|39622|6|Mentioned|p19|||||||||
17306|Staveley Formation|40840|6|Mentioned|Map legend|||||||||
17306|Staveley Formation|41272|6|Mentioned|M 1of1 H07|||||||||
17306|Staveley Formation|41306|3|Fully described|p11|||||||||
17306|Staveley Formation|41464|6|Mentioned|Map legend|Proterozoic||||||||
17306|Staveley Formation|41556|6|Mentioned|Map legend|Proterozoic||||||||
17306|Staveley Formation|41568|3|Fully described|p11|||||||||
17306|Staveley Formation|41791|6|Mentioned|p255|||||||||
17306|Staveley Formation|41978|6|Mentioned|p491|||||||||
17306|Staveley Formation|41979|6|Mentioned|Fig.2 P512|||||||||
17306|Staveley Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Sandstone, siltstone; commonly calcareous and ferruginous.||||||09-FEB-09
17306|Staveley Formation|43614|6|Mentioned|Fig.1|||||||||
17306|Staveley Formation|43620|6|Mentioned|Fig.1,p51|||||||||
17306|Staveley Formation|43767|5|Briefly described|p890|||||||||
17306|Staveley Formation|44271|2|Defined|p30,60|||Overlies Answer Slate.||||||
17306|Staveley Formation|44275|14|Not recorded|Map Legend|||||||||
17306|Staveley Formation|44276|2|Defined|p11,18,25,Tb.1,map|||||||||
17306|Staveley Formation|44277|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
17306|Staveley Formation|44279|14|Not recorded|Tb.1|||||||||
17306|Staveley Formation|44290|2|Defined|p438||Precambrian|||||||
17306|Staveley Formation|44788|14|Not recorded|p20|||||||||
17306|Staveley Formation|45161|4|Described|p48|||||||||
17306|Staveley Formation|45166|4|Described|p24|||||||||
17306|Staveley Formation|45287|14|Not recorded|p.225-7||Paleoproterozoic|||||||07-NOV-08
17306|Staveley Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy. Misspelling of Stavely?||||||
17306|Staveley Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
17306|Staveley Formation|49009|2|Defined|p44|Proterozoic|Proterozoic|See also p2.||||||02-APR-07
17306|Staveley Formation|49041|6|Mentioned|Table 4|||||||||
17306|Staveley Formation|50100|5|Briefly described|p11, p13 Fig. 4, p20|Statherian|Statherian|Well-bedded to locally brecciated calcareous, ferruginous, feldspathic, siliceous and micaceous sedim.rocks.  Unconformably overlies Kuridala Fm. (acc. to Donchak et al, 1983); overlain by Agate Downs Siltstone and Marimo Shale.  Geol. Prov: Eastern Fold Belt.||||||20-MAR-18
17306|Staveley Formation|50125|6|Mentioned|p86 Fig.1|||Geological Province: Mount Isa Inlier||||||
17306|Staveley Formation|50536|6|Mentioned|p11.4|||Geological Province: Mount Isa Inlier. Intruded by Gin Creek Granite.||||||
17306|Staveley Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mary Kathleen Group. Arenite, siltstone, phyllite, commonly calcareous and ferruginous.||||||
17306|Staveley Formation|60658|5|Briefly described|p61, p62 Fig.1|Proterozoic|Proterozoic|Of the Mary Kathleen Group.||||||
17306|Staveley Formation|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Isa Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||
17306|Staveley Formation|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
17306|Staveley Formation|61928|5|Briefly described|p114|||Metasedimentary rocks of the Mary Kathleen Group. Hosts the Starra Au-Cu orebodies.||||||
17306|Staveley Formation|61936|5|Briefly described|p190 Fig. 3|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.  See also p195 Fig. 6.||||||
17306|Staveley Formation|62047|6|Mentioned|p90 Fig.1 |||||||||
17306|Staveley Formation|64248|6|Mentioned|p36, p38 Fig.5|||Proposed inclusion in the informal Young Australia Group. Appears as Stavely on p36.||Mary Kathleen Group.||||11-DEC-17
17306|Staveley Formation|64250|5|Briefly described|p7, p13-15, p18, p20, p24, p27|||Cloncurry Fold Belt, Mount Isa Inlier.|1675-1610   or <1710 +/-20 Ma|Young Australia Group||Overlain by Marimo Slate and Agate Downs Siltstone (both conformably). Possible correlative of Mount Norna Quartzite.|Interbedded sandstone, siltstone, phyllite, shale and mudstone (variably calcareous, ferruginous, feldspathic and siliceous); minor metabasalt, conglomerate, felsic volcanics, marble, banded calc-silicate, and banded quartz-hematite-magnetite rock.|
17306|Staveley Formation|64253|6|Mentioned|p152 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: between ~1680-1610Ma. Geological Province: Mount Isa Block. term Formation is Fm in figure.||||||31-MAR-09
17306|Staveley Formation|65387|5|Briefly described|p3 Tb.1a|||Samples submitted but did not yield sufficient zircon for SHRIMP analysis.||Unit in Mary Kathleen Group.|||Includes possible felsic tuff.|
17306|Staveley Formation|65396|5|Briefly described|p7, p16-17, p82, p84, p169, p175, p178|Statherian|Statherian|See also p180, p182-184, p188-191, p195, p202, p241, p318, p439. The authors propose grouping this and other siliciclastic units of the Mary Kathleen Group into the informal Young Australia Group, now part of the Mount Albert Group. Isa Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. Also spelled Stavely Formation, Staverly Formation (p318). Detrital zircon sources listed.|1675 - 1610 Ma, <1710 +/- 20 Ma|Young Australia Group||Overlies Answer Slate, Kuridala Formation; and Double Crossing Metamorphics conformably. Conformably underlies Marimo Slate, Agate Downs Siltstone; is overlain by Roxmere Quartzite.|Interbedded sandstone, siltstone, phyllite, shale and mudstone. Minor marble, banded calc-silicate, banded-quartz hematite-magnetite rock, metabasalt, conglomerate and felsic metavolcanics.|04-APR-17
17306|Staveley Formation|66913|5|Briefly described|p170 fig 1, p172, 174, p176|||No reliable depositional ages.||||Correlated with Overhang Jaspilite, Doherty Formation, Corella Formation by some. Others correlate with Soldiers Cap Group.|Metasedimentary. Banded to brecciated calc-silicates.|
17306|Staveley Formation|67323|4|Described|p18-21, p24, p32-33, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Marimo-Staveley and Doherty-Fig Tree Gully Domains, Mount isa Inlier, Calvert Superbasin. Informally subdivided into 6 units. Includes rocks previously mapped as Doherty Formation (see p20-21). Sediments at least partly derived from Gin Creek Granite. Previously correlated with the Corella Formation but is younger than it. Low to moderate magnetic and gravity responses. Brecciated, generally folded, and metamorphosed to amphibolite facies. Also appears as Stavely on p19. A metarhyolite was dated at 1725 +/- 3 Ma (Page and Sun, 1998) but relationship is uncertain: if intrusive, it provides a minimum age. RELATED UNITS (continued): Is intruded by Toole Creek Volcanics, Williams Supersuite, Maramungee and Cowie Suites.|~1740 Ma (max. depositional age).|||Is overlain gradationally by Roxmere Quartzite. Probably underlies Soldiers Cap Group. Is faulted against Answer Slate and Double Crossing Metamorphics. See COMMENTS for intrusions.|Feldspathic to quartzose sandstone, siltstone and mudstone, locally calcareous and commonly hematitic; grading into scapolitic calc-silicate rocks; minor impure limestone and marble; local breccia.|
17306|Staveley Formation|67539|4|Described|p12, 13|||See also [mis-spelt] Stavely Formation p11, 12.||||Possible less altered equivalent of the Doherty Formation.||
17306|Staveley Formation|68146|5|Briefly described|p75, p91, p201|||Eastern Fold Belt, Mount Isa Inlier. Age determinations by Magee et al. (in press) and Neumann, unpublished OZCHRON respectively.|c.1784 Ma to 1743 Ma max. deposition age.|||Structurally overlies Double Crossing Metamorphics. Is overlain by Roxmere Quartzite. Probable lateral equivalent to part of Soldiers Cap Group.|Clast- to matrix-supported breccia of pinkish-grey, very fine-grained, slightly calcareous sandstone in a sandy calcareous matrix; passes westwards into thin- to thick-bedded calcareous sandstone and siltstone.|
17306|Staveley Formation|68542|4|Described|p16 fig 4, p17 fig 5|||More than 2000m thick.|1720 +/- 20 Ma|||Overlain by Kuridala Formation|Calcareous, ferruginous, feldspathic, micaceous and siliceous sandstones, siltstone, phyllite, marble. Lenses of breccia, schist and banded calc-silicate rocks, minor basalt and conglomerate.|
17306|Staveley Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. This unit is mapped with the Roxmere Quartzite under the symbol, -Ps.||||||
17306|Staveley Formation|68575|4|Described|p2-3, p6-7, p60-74, p125-126, p134|||Mount Isa Region. Includes a metamorphosed and metasomatised subunit previously mapped as part of the Doherty Formation; two samples with maximum depositional ages of 1780 +/- 10 Ma and 1749 +/- 4 Ma probably reflect different provenances. Diverse provenance: youngest population possibly from Argylla Formation. Whole rock Sm-Nd isotopic data and ages (1784 Ma, 1749 Ma).|c.1780 Ma; c.1749 Ma.|||Is faulted against Double Crossing Metamorphics.|Pink to brown, fine-grained, thinly bedded sandstone.|
17306|Staveley Formation|68576|5|Briefly described|Q_2: p16-18|||Part of Cover Sequence 2 or 3 of the Eastern Fold Belt, Mount Isa Inlier. Associated with IOCG mineralisation. Occurs west of the Mount Dore fault. Over 2000m thick linear belt of well-bedded to brecciated, shallow-water sediments. Intruded by several dykes and sills.|<1720 +/- 20 Ma.||||Variably calcareous, ferruginous, feldspathic, micaceous and siliceous sandstone, siltstone and phyllite, impure limestone (marble), schist and banded calc-silicate rocks; minor basalt, conglomerate, quartz-magnetite-hematite ironstones.|
17306|Staveley Formation|69056|4|Described|p2, p4-6, p9, p11, p13, p18, p23, p28|Statherian|Statherian|See also p37, p54-55, Reference images sheet, Time-Space plot sheet. Shown on the simplified surface and solid geology maps of the Quamby Project area; mapped as one unit with Roxmere Quartzite. Includes rocks previously mapped as Doherty Formation (now obsolete) and Corella Formation. Contact with Soldiers Cap Group plays a significant role in epigenetic Cu-Au-Fe oxide mineralisation. Modelling values listed. Maximum deposition age range cluster (Magee et al., 2012). Various 'maximum age from detrital zircon' values given, but 1725 +/-3 Ma age is shown as from a felsic igneous unit near the base (See Time-Space Plot)|~1750 - 1740 Ma maximum depositional age..||Gilded Rose Breccia.|Overlies Bulonga Volcanics (basement in Soldiers Cap Domain). Is overlain by Soldiers Cap Group or Roxmere Quartzite. Staveley Formation is thust over the Soldiers Cap Group in places.|Siltstone, sandstone, sandy carbonate and calc-silicate rocks.|20-MAR-18
17306|Staveley Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block.||||Overlies Kuridala Formation and Answer Slate. Is overlain by Marimo Slate.||25-JAN-19
17306|Staveley Formation|69377|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Very thinly interbedded sandstone and siltstone, variably calcareous with local impure limestone and calc-silicate rocks; local areas of breccia|
17306|Staveley Formation|69378|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Very thinly interbedded sandstone and siltstone, variably calcareous with local impure limestone and calc-silicate rocks; local areas of breccia|
17306|Staveley Formation|69591|4|Described|p29, p37-39, p40 Figs.2.25-26, p41|Paleoproterozoic|Paleoproterozoic|See also p46, p49, p51-52, p56, p106-107. Marino-Staveley Domain, Mount Isa Province. Part of the ?Big Supersequence. Shallow-marine deposits. Separated from the underlying Gin Creek Granite and Double Crossing Metamorphics by an inferred folded decollement. Includes rocks previously mapped as Doherty Formation. Forms an imbricate thrust belt of narrow, alternating linear belts with Answer Slate. Some calc-silicate breccias (probably formed by fluidisation from late-Isan Orogeny magmatism) intrude the Soldiers Cap Group as dyke- and plug-like masses.|1725 +/- 3 Ma (Neumann et al., 2009).|||Is overlain gradationally by Roxmere Quartzite. Is faulted against Answer Slate.|Includes very thinly-bedded and ripple cross-laminated sandstone, and cross-laminated sandstone with interbedded calcareous beds with extensive scapolite replacement. Breccias widespread.|
17306|Staveley Formation|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Four facies are mapped separately.||Mount Albert Group.||Is overlain by Roxmere Quartzite.|Sandstone and siltstone, variably calcareous; local impure limestone, calc-silicate rocks; matrix-supported breccias of calcareous sandstone and siltstone; local massive ironstone lenses.|
17306|Staveley Formation|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Four facies are mapped separately.||Mount Albert Group.||Is overlain by Roxmere Quartzite.|Sandstone and siltstone, variably calcareous; local impure limestone, calc-silicate rocks; matrix-supported breccias of calcareous sandstone and siltstone; local massive ironstone lenses.|
17306|Staveley Formation|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Three facies associations are mapped separately.||Mount Albert Group.|||Interbedded sandstone and siltstone, variably calcareous; matrix-supported breccias of calcareous sandstone and siltstone (+/- calc-silicate rock); local impure limestone.|
17306|Staveley Formation|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Three facies associations are mapped separately.||Mount Albert Group.|||Interbedded sandstone and siltstone, variably calcareous; matrix-supported breccias of calcareous sandstone and siltstone (+/- calc-silicate rock); local impure limestone.|
17306|Staveley Formation|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Five facies associations are mapped separately.||Mount Albert Group.||Is overlain by Roxmere Quartzite. Intruded by Wiggle Waterhole Metagabbro.|Banded scapolitic calc-silicate granofels and subordinate impure marble; metasomatised rocks; metadolerite and amphibolite bodies. Breccia: calcareous sandstone/siltstone/calc-silicate rock, matrix supported. Interbedded sandstone and siltstone.|05-MAY-16
17306|Staveley Formation|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes three unnamed members; banded scapolitic calc silicate granofels, matrix supported breccia of calcareous sandstone and a very thinly interbedded sandstone and siltstone.||Mount Albert Group.|Includes three unnamed members.|Intruded by Wiggle Waterhole Metagabbro.||
17306|Staveley Formation|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Intruded by Wiggle Waterhole Metagabbro.|Metasomatised calc-silicate granofels, commonly brecciated, minor areas of coherent, banded calc-silicate granofels.|20-JAN-22
17306|Staveley Formation|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||Mount Albert Group.||Intruded by Wiggle Waterhole Metagabbro.|Metasomatised calc-silicate granofels, commonly brecciated; minor areas of coherent, banded calc-silicate granofels.|
17306|Staveley Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1710+/-20 Ma (MDA: U-Pb zircon SHRIMP)||||Schist.|
17306|Staveley Formation|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block.|ca 1725 Ma|||Overlain by the Roxmere Quartzite.|Dolomite, calc-silicate rocks.|
17306|Staveley Formation|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain, Kuridala-Selwyn Domain, and  Doherty-Fig Tree Gully Domain. Comprised of 4 informal lithological divisions variably calcareous with local impure limestone and calc-silicate rocks; local areas of breccia. Banded scapolitic calc-silicate granofels and subordinate impure marble.||Mount Albert Group||Underlies Roxmere Quartzite in Marimo-Staveley Domain.|Banded scapolitic calc-silicate granofels and subordinate impure marble; locally abundant breccia and metasomatised rocks; metadolerite and amphibolite bodies common. Thinly interbedded sandstone and siltstone, variably calcareous. Local breccia.|
17306|Staveley Formation|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Marimo-Staveley Domain, Kuridala-Selwyn Domain, and  Doherty-Fig Tree Gully Domain. Comprised of 4 informal lithological divisions variably calcareous with local impure limestone and calc-silicate rocks; local areas of breccia. Banded scapolitic calc-silicate granofels and subordinate impure marble.||Mount Albert Group||Underlies Roxmere Quartzite in Marimo-Staveley Domain.|Banded scapolitic calc-silicate granofels and subordinate impure marble; locally abundant breccia and metasomatised rocks; metadolerite and amphibolite bodies common. Thinly interbedded sandstone and siltstone, variably calcareous. Local breccia.|
17306|Staveley Formation|72889|5|Briefly described|p2, p5, p8, p27-31.|Calymmian|Calymmian|The maximum depositional age range reported in Neumann, Geochron Delivery-a; (Withnall, 2019)|c. 1755-1743 Ma.|||Possibly intruded by Gin Creek Granite, but more likely younger because grades transitionally into Roxmere Quartzite. May correlate with Corella Formation?|Includes brecciated and hematised calc-silicate rocks.|
17306|Staveley Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
17306|Staveley Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Kuridala-Selwyn-Marimo-Doherty and Snake Creek-Soldiers Cap Domain.|1785+/-11 Ma, ~1750 Ma, 1710+/-10 Ma MDA||||Carbonates, includes felsic extrusives, siliciclastics and metamorphics.|
17310|Steamboat Sandstone|12951|5|Briefly described|p143 fig 4, 148|Middle Cambrian|Middle Cambrian|Georgina Basin. Overlying Arthur Creek Formation or Member at top?||?of Arthur Creek Formation.|||Quartzitic dolostone and dolomitic sandstone.|
17310|Steamboat Sandstone|24419|5|Briefly described|p18, p19|Late Cambrian|Middle Cambrian|Cross-stratified, ripple marked sandstone with interbedded silty sandstone and siltstone and basal units of sandy limestone and limestone. Erosional contact with underlying Quita Formation. Geological Province: Georgina Basin.||||||
17310|Steamboat Sandstone|24442|5|Briefly described|p45, p49|Middle Cambrian|Middle Cambrian|Quartzic dolostone and quartz sandstone.  Overlies the Arthur Creek Formation.  On SANDOVER RIVER sheet.||||||
17310|Steamboat Sandstone|30242|6|Mentioned|Fig.2|||||||||
17310|Steamboat Sandstone|30479|6|Mentioned|Fig.6|||Stratigraphic relationships||||||
17310|Steamboat Sandstone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17310|Steamboat Sandstone|31287|6|Mentioned|p430|||Refers Opik (1956)||||||
17310|Steamboat Sandstone|33111|6|Mentioned|Fig.15|||||||||
17310|Steamboat Sandstone|34287|6|Mentioned|Fig.3|||||||||
17310|Steamboat Sandstone|34847|6|Mentioned|p40|||Also Table 1, stratigraphy & hydrocarbon prospects.||||||
17310|Steamboat Sandstone|35054|6|Mentioned|Table 23|||||||||
17310|Steamboat Sandstone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
17310|Steamboat Sandstone|35139|4|Described|Table.2|||||||||
17310|Steamboat Sandstone|35553|6|Mentioned|p8|||See also Appendix 2, description of Agnostid localities.||||||
17310|Steamboat Sandstone|36234|6|Mentioned|p175|||||||||
17310|Steamboat Sandstone|37572|4|Described|p158|||See also Fig.8||||||
17310|Steamboat Sandstone|38442|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Middle to Late? Cambrian||||||25-AUG-04
17310|Steamboat Sandstone|38446|6|Mentioned|Table 23|||||||||
17310|Steamboat Sandstone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
17310|Steamboat Sandstone|39445|5|Briefly described|Table 4|||See also P62||||||
17310|Steamboat Sandstone|44205|4|Described|p46,47|||=age of Roaring Siltstone and Devoncourt Limestone.||||||
17310|Steamboat Sandstone|44211|14|Not recorded|p93,95-97,101-107|||Rests with breakd on Quita Formation.||||||
17310|Steamboat Sandstone|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
17310|Steamboat Sandstone|44275|14|Not recorded|Map Legend|||||||||
17310|Steamboat Sandstone|44309|2|Defined|Tb.1,p7,8-10,17||Middle Cambrian|Interfingers with Mungerebar Limestone above.||||||
17310|Steamboat Sandstone|44326|14|Not recorded|Map Legend||Middle Cambrian|||||||
17310|Steamboat Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Middle Cambrian|||||||
17310|Steamboat Sandstone|45002|14|Not recorded|p24|||early Late Cambrian fossils deposited in agitated shallow water, food abundant. See also Lexicon.||||||
17310|Steamboat Sandstone|45012|14|Not recorded|p1-9,16,19,26,28,91,||Middle Cambrian|p133-35,173-77,300-304,332-366||||||
17310|Steamboat Sandstone|45052|3|Fully described|p101|||M.Camb.||||||
17310|Steamboat Sandstone|45054|6|Mentioned|p5|||Fossil locality||||||
17310|Steamboat Sandstone|45079|4|Described|p38|||Cambrian age||||||
17310|Steamboat Sandstone|45119|6|Mentioned|p4|||||||||
17310|Steamboat Sandstone|45166|5|Briefly described|Table 15|||||||||
17310|Steamboat Sandstone|45168|6|Mentioned|p6|||||||||
17310|Steamboat Sandstone|46959|6|Mentioned|Table 1|||||||||
17310|Steamboat Sandstone|47024|6|Mentioned|Table 1|||||||||
17310|Steamboat Sandstone|47058|6|Mentioned|p136|||||||||
17310|Steamboat Sandstone|48633|14|Not recorded|p96|||Ref. to Opik 1961.||||||
17310|Steamboat Sandstone|60122|4|Described|p18|Middle Cambrian|Middle Cambrian|Conformably on Arthur Creek Formation; conformable beneath Arrintrhunga Formation and Mungerebar Limestone. Possible disconformable on Quita Fm. in URANDANGI-GLENORMISTON. Max. thick: 80m. Geol.Prov: Georgina Basin. See also p405, p11 Tb. 1.||||||
17310|Steamboat Sandstone|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 80m. Conformably underlies: Arrinthrunga Formation. Conformably overlies: Arthur Creek Formation. Possibly disconformably overlying Quita Formation.||||||08-MAR-23
17310|Steamboat Sandstone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Sandstone, siltstone.||||||
17310|Steamboat Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and calcareous/dolomitic quartz sandstone, quartzose dolostone.  Conformably overlies the Arthur Creek Formation; conformably overlain by Arrinthrunga Formation.||||||26-NOV-04
17310|Steamboat Sandstone|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and calcareous/dolomitic quartz sandstone, quartzic dolostone.||||||
17310|Steamboat Sandstone|61022|5|Briefly described|p14, p15||Cambrian|Near-shoreline (tidal channel and deltaic clastics) oolitic carbonate and quartz-rich sandstone. Potential to trap oil in sediments below. Geological Province: Georgina Basin.||||||20-APR-05
17310|Steamboat Sandstone|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems - potential reservoirs up to 150m thick.  Geological Province: Georgina Basin.||||||18-AUG-05
17310|Steamboat Sandstone|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Narpa Group. Quartzose and calcareous/dolomitic quartz sandstone, quartzose dolostone. Geological Province: southern Georgina Basin.||||||11-OCT-05
17310|Steamboat Sandstone|62759|5|Briefly described|p1|||Overlies Arthur Creek Formation. Geological Province: Georgina Basin.||||||05-FEB-08
17310|Steamboat Sandstone|64068|4|Described|p64-65, p62, 63, 67, 69, p88-89, p ix|Middle Cambrian|Middle Cambrian|Diverse trilobite fauna. Correlated with Devoncourt Limestone, lower Georgina Limestone, Cleland Sandstone in part, Illara Sandstone, Hugh River Shale in part, Shannon Formation in part, Petermann Sandstone.||Of Narpa Group.||Overlies Quita and Arthur Creek Formations. Laterally interdigitates with and conformably overlain by Mungerebar Limestone, Arrinthrunga Formation.|Quartz and calcareous sandstones with interbeds of quartzic grainstone and quartz dolostone; minor siltstone.|05-APR-12
17310|Steamboat Sandstone|64443|6|Mentioned|p9, p17, p18|Late Cambrian||An uppermost portion of the Arthur Creek Formation may alternatively represent this unit; a probable correlative of the quartz sandstone Cmdz unit (uppermost Camooweal Dolostone).||||. Conformably underlies Arrinthrunga Formation.||14-MAY-14
17310|Steamboat Sandstone|64812|4|Described|p236, p241-2 Fig. 8, 9, p243, p247|Late Cambrian|Late Cambrian|The inner ramp facies caps/interfingers with upper Arthur Creek Fm middle ramp facies; may be unconformable with overlying Chabalow/Arerinthrunga Fms. Near-shoreline oolitic carbonate + quartz-rich sandstone - more lith.details. Geol.Prov:Georgina Basin.||||||07-FEB-11
17310|Steamboat Sandstone|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Overlies/interfingers with Arthur Creek Formation. Geological province: Georgina Basin. Near-shore quartz clastic rocks.||||||11-FEB-09
17310|Steamboat Sandstone|65237|4|Described|p3 Fig. 4, p8|Middle Cambrian|Middle Cambrian|Overlies Chabalowe and Arrinthrunga Formations, usually conformably. Max. thickness: 250m. Geol.prov: southern Georgina Basin.Near-shoreline calcareous/siliciclastic sandstone, interbedded with oolitic rocks which interfinger with upper Arthur Creek Fm.||||||07-FEB-11
17310|Steamboat Sandstone|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||||Overlies Arthur Creek Formation.||
17310|Steamboat Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Middle Cambrian|Middle Cambrian|Georgina Basin||Narpa Group|||Calcarenite, calcareous and quartzose arenite, calcilutite|
17310|Steamboat Sandstone|69437|5|Briefly described|p22:10|Series 3|Series 3|Southern Georgina Basin. Potential petroleum reservoir.||||Overlies Arthur Creek Formation. Is overlain by Arrinthrunga Formation.||12-JUL-16
17310|Steamboat Sandstone|69443|4|Described|p28:16-19, 31|Middle Cambrian|Middle Cambrian|Noakes et al. (1959). Southern Georgina Basin. Forms mesa caps and plains. 17-221m thick. Diverse trilobite fauna: Boomerangian age. Nearshore sand to shallow-marine platform-edge deposits.||Narpa Group.||Conformably overlies Arthur Creek and Quita Formations. Is overlain conformably by Arrinthrunga Formation and Mungerebar Limestone (with which it interdigitates).|Quartz sandstone and calcareous sandstone, with interbeds of quartzose grainstone and quartzose dolostone; minor siltstone.|12-JUL-16
17310|Steamboat Sandstone|69561|6|Mentioned|p33 fig 2|Boomerangian|Boomerangian|||||Overlain by Arrinthrunga Formation, overlies Arthur Creek Formation||
17310|Steamboat Sandstone|69573|6|Mentioned|p659, 661, 666|||Georgina Basin. Intertidal to subtidal environment.||||||
17310|Steamboat Sandstone|69591|5|Briefly described|p87, p91, p96|Cambrian|Cambrian|Oban Sub-basin, Georgina Basin. Up to 80m thick. Trilobite fauna indicates late middle Cambrian (Lejopyge laevigata Zone).||||Overlies Quita Formation transitionally. Is overlain by and interfingers with Mungerebar Limestone.|Calcareous and quartz sandstones with interbeds of sandy limestone and dolomite; locally, the upper 25m has leached sandstone and minor siltstone.|
17310|Steamboat Sandstone|69673|5|Briefly described|p116, p117, p127, p129, p133, p138|||Up to 221m thick. Trilobite fossils present. Potential as a reservoir rock.||Narpa Group||Conformably overlies Arthur Creek Formation, conformably overlain by Arrinthrunga Formation|Quartz sandstone and calcareous sandstone with interbeds of grainstone and quartzic dolostone with minor siltstone.|
17310|Steamboat Sandstone|70380|6|Mentioned|p745|Series 3|Series 3|Southern Georgina Basin.||||||
17310|Steamboat Sandstone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group||Overlies Quita Formation and Arthur Creek Formation. Is overlain by Mungerebar Limestone, Arrinthrunga Formation.|Sandstone.|
17310|Steamboat Sandstone|70951|5|Briefly described|p1083|||Geological province: Georgina Basin.||||Underlain by Arthur Creek Formation. Overlain by Hagen Member.||
17310|Steamboat Sandstone|72321|5|Briefly described|Fig 2, p4, p6|Guzhangian|Guzhangian|Toko Syncline, Georgina Basin. New, younger age based on Boomerangian agnostid trilobites in underlying Arthur Creek Foramtion. Australian Stage: upper Boomerangian.||of Narpa Group.||Overlies Arthur Creek Formation in Toko Syncline. May correlate with Chabalowe Formation, Dulcie Syncline.||
17310|Steamboat Sandstone|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites.||Narpa Group||Overlain by the Arrinthrunga Formation including the Eurowie Sandstone Member. Overlies the Arthur Creek Formation.|Quartz sandstone, calcareous sandstone, interbeds of quartzitic grainstone, quartzitic dolostone and minor siltstone.|05-JUL-22
17310|Steamboat Sandstone|72516|3|Fully described|p11-12, p92-93|Cambrian Series 3|Cambrian Series 3|Georgina Basin. Previously included in the Arthur Creek Formation before being separated by Dunster et al (2007). Occurs on GLENORMISTON, URANDANGI, SANDOVER RIVER, TOBERMORY and HUCKITTA map sheets; subsurface occurences are known in MOUNT WHELAN. Outcrops on the Jervois Range Special occur north of the Johannsen Range and west of the Jervois Range where it forms mesa caps and plains. Contains fossil trilobites which indiacte an upper Series 3 Cambrian age. Deposited in a near-shore, shallow marine; possibly barrier bar system. 40m thick in the mapped area, 17-221m elsewhere. Part equivalent of the Cleland Sandstone, Illara Sandstone, Hugh River Shale, Shannon Formation and the Petermann Sandstone.||Narpa Group||Conformably and gradationally overlain by the Arrinthrunga Formation. Conformably overlies the Arthur Creek Formation. Equivalent to the Devoncourt Limestone and the Georgina Limestone.|Quartz sandstone, calcareous sandstone; interbeds of quartzitic grainstone, quartzitic dolostone, minor siltstone.|03-JUN-21
17310|Steamboat Sandstone|73083|6|Mentioned|p75|Late Cambrian|Middle Cambrian|||||||
17310|Steamboat Sandstone|73288|5|Briefly described|p702|||Southern Georgina Basin. Downhole (Hylogger) logs.||||Overlies Arthur Creek Formation. Is overlain by Hagen Member.||
17312|Steamers Trachyte Member|39969|6|Mentioned|p9|||||||||
17312|Steamers Trachyte Member|42485|6|Mentioned|p264|||||||||
17312|Steamers Trachyte Member|48917|6|Mentioned|p7|||Refers Stevens (1965)||||||
17312|Steamers Trachyte Member|73450|6|Mentioned|p92|||||Governors Chair Volcanics|||Felsic.|
17319|Stenhouse Creek Amphibolite|22533|6|Mentioned|p55|||In Georgetown Region||||||
17319|Stenhouse Creek Amphibolite|23032|4|Described|p12|||||||||
17319|Stenhouse Creek Amphibolite|23291|5|Briefly described|p30|Early Paleozoic|Proterozoic|Parent: Boiler Gully Complex. Geological Province: Georgetown Region.||||||08-JUL-15
17319|Stenhouse Creek Amphibolite|23494|5|Briefly described|p9, p25 Tb. 1|Archean|Archean|Banded amphibolite.  Conformably overlies Hall's Reward Metamorphics.||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|23616|6|Mentioned|Table 1C p16|||Probably equivalent to Sandalwood Serpentinite||||||
17319|Stenhouse Creek Amphibolite|23619|4|Described|p43 Table 2||Proterozoic|Originally thought to be older than Boiler Gully Complex.  Of Boiler Gully Complex. Georgetown Province.||||||
17319|Stenhouse Creek Amphibolite|29446|6|Mentioned|p120|||||||||
17319|Stenhouse Creek Amphibolite|31832|6|Mentioned|Table 6|||||||||
17319|Stenhouse Creek Amphibolite|37768|6|Mentioned|p34|||||||||
17319|Stenhouse Creek Amphibolite|41675|4|Described|p17|||||||||
17319|Stenhouse Creek Amphibolite|42407|5|Briefly described|p33|||||||||
17319|Stenhouse Creek Amphibolite|42692|5|Briefly described|map legend|Proterozoic||||||||
17319|Stenhouse Creek Amphibolite|42693|5|Briefly described|map legend|Mesoproterozoic|Early Paleozoic|||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|43060|6|Mentioned|p35|||||||||
17319|Stenhouse Creek Amphibolite|43113|4|Described|Table 2 p28||Proterozoic|of Boiler Gully Complex||||||
17319|Stenhouse Creek Amphibolite|43253|5|Briefly described|map legend||Proterozoic|Early to Middle Proterozoic age. Of Boiler Gully Complex.||||||
17319|Stenhouse Creek Amphibolite|43286|5|Briefly described|Map Legend||Proterozoic|of Boiler Gully Complex.||||||
17319|Stenhouse Creek Amphibolite|43716|6|Mentioned|p130|||||||||
17319|Stenhouse Creek Amphibolite|44043|14|Not recorded|Fig.8,66-7,69-70,73||Archean|Overlain by Halls Reward Metamorphics.||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|44048|14|Not recorded|Map Legend||Archean|||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|44059|2|Defined|p443,446||Archean|||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|45009|2|Defined|p26-7,79,115|||Member of Halls Reward Metamorphics?.||||||
17319|Stenhouse Creek Amphibolite|45151|5|Briefly described|Table 4|||||||||
17319|Stenhouse Creek Amphibolite|48904|6|Mentioned|Table 2|||Correlation||||||
17319|Stenhouse Creek Amphibolite|50202|5|Briefly described|Map legend|Early Paleozoic|Neoproterozoic|Of the Boiler Gully Complex.  Amphibolite, metagabbro and minor clinopyroxinite.||||||07-NOV-08
17319|Stenhouse Creek Amphibolite|67455|5|Briefly described|p575 Table 1, pp591-592.|||Halls Reward domain, Greenvale Province. May represent oceanic crust.||Unit in Boiler Gully Complex.|||Layered amphibolite, interbedded with metagabbro of Sandalwood Serpentinite. Shortened to Stenhouse Amphibolite p.591.|04-MAY-12
17319|Stenhouse Creek Amphibolite|68336|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.||Unit in Boiler Gully Complex.|||Amphibolite, metagabbro and minor clinopyroxenite.|
17319|Stenhouse Creek Amphibolite|68341|5|Briefly described|Map legend.|Cambrian?|Neoproterozoic?|Cape River Province.||Unit in Boiler Gully Complex.|||Amphibolite, metagabbro and minor clinopyroxenite.|
17319|Stenhouse Creek Amphibolite|68344|5|Briefly described|Map legend.|Early Paleozoic?|Neoproterozoic|Cape River Province.||Unit in Boiler Gully Complex.|||Amphibolite, metagabbro and minor clinopyroxenite.|
17319|Stenhouse Creek Amphibolite|68731|5|Briefly described|p156|Cambrian|Cambrian|Relict igneous textures are shown by plagioclase laths and relict clinopyroxene in metagabbro. Age constrained by the parent Boiler Gully Complex.||Of the Boiler Gully Complex.|||Comprises amphibolite, metagabbro and some clinopyroxene. The amphibolite and metagabbro consist of hornblende, plagioclase and epidote. Clinopyroxene consists of clinopyroxene replaced partly or wholly by tremolite.|
17324|Stephens Formation|41809|6|Mentioned|p64|||||||||
17326|Stevenson Quartz Monzodiorite|42747|5|Briefly described|Fig.9 P38|||see also Table 1 P37. Reserved as Stevenson Monzonite.||||||
17326|Stevenson Quartz Monzodiorite|43029|2|Defined|p15||Middle Devonian|Rb-Sr age of 382 Ma,see also Fig.2,p16||||||
17326|Stevenson Quartz Monzodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
17326|Stevenson Quartz Monzodiorite|43213|3|Fully described|p96-97, p103, p116-121, p170, p174-175|Middle Devonian|Middle Devonian|See also p179, p208, p210-211, p222-223, p231, p240, p242. Type locality described. Component of the Retreat Batholith. Also a Rb-Sr biotite-whole rock pair age of 382 +/- 3 Ma (Carr, pers. comm., 1993). Geochemistry, modal and chemical analyses and geophysics detailed. Strongly magnetic.|379 Ma (K-Ar; Webb and McDougall, 1968).|||Intrudes Anakie Metamorphic Group. Is overlain unconformably by Silver Hills Volcanics.|Dark to light grey, fine- to coarse-grained, (sub-)equigranular biotite-hornblende quartz monzonite to biotite-hornblende quartz diorite.|
17326|Stevenson Quartz Monzodiorite|69952|5|Briefly described|p115|Devonian|Devonian|K-Ar and Rb-Sr biotite ages.|c.382-c.379 Ma.|||||
17351|Stockyard Creek Mudstone Member|23291|4|Described|p85 Tb. 3.6|Paleoproterozoic|Paleoproterozoic|Parent: Etheridge Group. Age: <1650Ma (U-Pb zircon). Thickness: 50-300m. Geological Province: Georgetown Region.||||||13-MAY-15
17351|Stockyard Creek Mudstone Member|23425|5|Briefly described|p371|||of Etheridge Group, Etheridge Province.||||||
17351|Stockyard Creek Mudstone Member|23430|6|Mentioned|p450|||||||||
17351|Stockyard Creek Mudstone Member|39917|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
17351|Stockyard Creek Mudstone Member|40218|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
17351|Stockyard Creek Mudstone Member|41975|5|Briefly described|Table 1 P434|||See also P437||||||
17351|Stockyard Creek Mudstone Member|43664|4|Described|p34|||||||||
17351|Stockyard Creek Mudstone Member|43665|5|Briefly described|p13||Proterozoic|||||||
17351|Stockyard Creek Mudstone Member|50210|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Candlow Formation.||||||07-NOV-08
17351|Stockyard Creek Mudstone Member|50537|6|Mentioned|p2.5, Table 2.1|||Of the Etheridge Group. Geological Province: Georgetown Inlier.||||||19-AUG-04
17351|Stockyard Creek Mudstone Member|50595|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Candlow Formation. Carbonaceous mudstone.||||||07-NOV-08
17351|Stockyard Creek Mudstone Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Georgetown Inlier.||Candlow Formation.||||
17351|Stockyard Creek Mudstone Member|67341|6|Mentioned|vi|||Forsayth Subprovince, Etheridge Province.||Candlow Formation.||||
17351|Stockyard Creek Mudstone Member|68348|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Dark grey to black, pyritic carbonaceous mudstone; rare quartz-albite rock.|13-MAY-15
17351|Stockyard Creek Mudstone Member|68349|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Dark grey to black, pyritic carbonaceous mudstone; rare quartz-albite rock.|13-MAY-15
17351|Stockyard Creek Mudstone Member|68352|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Has reverse remnnant magnetisation. Min Age: Mesoproterozoic?||Unit in Candlow Formation.|||Dark grey to black, pyritic carbonaceous mudstone; rare quartz-albite rock.|18-MAY-15
17351|Stockyard Creek Mudstone Member|68355|5|Briefly described|Map legend.||Paleoproterozoic|Etheridge Province. Age min: Mesoproterozoic?||Unit in Candlow Formation.|||Dark grey to black, pyritic carbonaceous mudstone; rare quartz-albite rock.|04-JUN-15
17351|Stockyard Creek Mudstone Member|68415|5|Briefly described|Map Legend|Calymmian|Statherian|Shown as younger than 1650 Ma and and older than D1 (> 1560 Ma, < 1590? Ma).|~ 1650-1560 Ma|Of the Candlow Formation.|||Dark grey to black, pyritic carbonaceous mudstone; rare quartz-albite rock.|
17351|Stockyard Creek Mudstone Member|69591|5|Briefly described|p65-66|Paleoproterozoic|Paleoproterozoic|Suggested depositional environments include deep-water sediments or turbidites.||Candlow Formation.|||Distinctive carbonaceous mudstone.|
17378|Stony Range Basalt|42895|3|Fully described|p58|||||||||
17378|Stony Range Basalt|68421|5|Briefly described|Map Legend|Zanclean|Zanclean|Bundaberg Volcanic Province. K-Ar (whole rock) age.|4.86 +/- 0.08 Ma (Robertson, 1992).||||Nephelinite, basanite and hawaiite commonly containing megacrysts and xenoliths of lherzolite.|
17386|Storm Hill Sandstone|23032|5|Briefly described|p28 fig6|Devonian|Devonian|||||||
17386|Storm Hill Sandstone|23424|5|Briefly described|Table 8.1 p335|Givetian|Emsian|Wando Vale Subgroup/Broken River Group. Graveyard Creek Subprovince.||||||
17386|Storm Hill Sandstone|23522|5|Briefly described|p250 Fig 6|Eifelian|Eifelian|||||||
17386|Storm Hill Sandstone|24577|4|Described|p752 Fig. 1, p754 Fig. 2|Givetian|Pragian|Of the Broken River Group. Overlain by the Dosey Limestone. Overlies the Lomandra Limestone and the Bracteata Formation. Sandstone is Ss in text. Geological Province: Broken River Region, Lachlan Fold Belt.||||||
17386|Storm Hill Sandstone|41260|4|Described|Table 1|||Reserved as Storm Hill Formation||||||
17386|Storm Hill Sandstone|41679|2|Defined|p258|Eifelian|Emsian|Age: Emsian to late Eifelian.||||||
17386|Storm Hill Sandstone|41719|6|Mentioned|Fig.2|||||||||
17386|Storm Hill Sandstone|41739|6|Mentioned|Fig.2|||||||||
17386|Storm Hill Sandstone|41740|6|Mentioned|p222|||||||||
17386|Storm Hill Sandstone|42031|5|Briefly described|Fig.5 P762|||||||||
17386|Storm Hill Sandstone|42032|6|Mentioned|p505|||See also Fig.12||||||
17386|Storm Hill Sandstone|42054|6|Mentioned|p273|||||||||
17386|Storm Hill Sandstone|42693|5|Briefly described|map legend|Middle Devonian|Early Devonian|||||||
17386|Storm Hill Sandstone|42709|6|Mentioned|map legend|||||||||
17386|Storm Hill Sandstone|42933|3|Fully described|Table 2|||See also p104||||||
17386|Storm Hill Sandstone|50093|3|Fully described|p237, p329 Fig.2|Eifelian; kockelianus zone (conodont)|Emsian; inversus zone (conodont)|Max. Thickness: 184 m. Horizontally stratified + cross-bedded, very coarse grained arenites. Overlies Bracteata Fm + Lomandra Limestone + onlaps Judea Fm, conformably overlain by Dosey Limestone. Of Broken River Gp.||||||07-FEB-11
17386|Storm Hill Sandstone|65214|6|Mentioned|p278|Devonian|Devonian|QLD, Broken River. Appears as Storm-hill Sandstone. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17386|Storm Hill Sandstone|68336|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Quartzose to subfeldspathic sandstone and pebble to granule conglomerate.|
17386|Storm Hill Sandstone|68341|5|Briefly described|Map legend.|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Unit in Wando Vale Subgroup.|||Quartzose to subfeldspathic sandstone and pebble to granule conglomerate.|
17386|Storm Hill Sandstone|68478|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Quartzose to subfeldspathic sandstone and pebble to granule conglomerate.|
17386|Storm Hill Sandstone|68479|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Graveyard Creek Subprovince.||Of the Wando Vale Subgroup.|||Quartzose to subfeldspathic sandstone and pebble to granule conglomerate.|
17386|Storm Hill Sandstone|69592|5|Briefly described|p264, p266|||Southern Graveyard Creek Subprovince, Broken River Province. Thickness in measured sections is <100m; locally much thicker. Nearshore fan delta deposits spreading onto a shallow shelf.||Wandovale Subgroup.||Conformably overlies Lomandra Limestone or, where mising, Bracteata Mudstone; locally Judea Formation unconformably. Is overlain by Dosey Limestone.|Granular to pebbly, feldspathic to quartzose, coarse- to very coarse-grained sandstone and polymict conglomerate. Contains poorly preserved moulds of diverse fossil fauna.|
17459|Stud Formation|23422|5|Briefly described|p180, p206 Table 6.3|Late Devonian|Late Devonian|Of Dotswood Group.||||||
17459|Stud Formation|23430|5|Briefly described|Plate 14.11 + p505||Devonian|Of Dotswood Group. Overlain by Julia Formation; underlain by Vanneck Formation. In the Burdekin Basin Province.||||||28-NOV-06
17459|Stud Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Dotswood Group.||||||19-FEB-07
17459|Stud Formation|23522|5|Briefly described|p250 Fig 6|Famennian|Givetian|||||||
17459|Stud Formation|23893|5|Briefly described|p16|Late Devonian|Late Devonian|Of Dotswood Group. Geological Province: Burdekin Basin.||||||08-JUL-15
17459|Stud Formation|24577|4|Described|p752 Fig. 1, p755 Fig. 2|Frasnian|Frasnian|Of the Dotswood Group. Overlain by the Julia Formation. Overlies the Vanneck Formation. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||
17459|Stud Formation|24613|2|Defined|p9 Fig. 4, p39-40|Frasnian|Frasnian|Contains Yarraman Sst Member. Conformable on Vanneck Fm; conformable below Julia Fm. Max. thickness: 800m. Geol.prov: Burdekin Basin.Lower + upper dominantly fine-gr.redbed deposits separated by the middle dominantly sandstone member.Detailed lith.incl.||||||07-FEB-11
17459|Stud Formation|24614|5|Briefly described|p191 Fig. 1|Famennian|Frasnian|Of the Dotswood Group. Geological Province: Burdekin Basin.||||||07-FEB-11
17459|Stud Formation|31285|4|Described|p82|||See also p88. Frasnian. Unit of Dotswood Gp.||||||19-FEB-07
17459|Stud Formation|37573|4|Described|p210|||See also Figs.7 and 8.||||||19-FEB-07
17459|Stud Formation|39445|5|Briefly described|Table 6|||||||||
17459|Stud Formation|39686|4|Described|p79|||||||||
17459|Stud Formation|42689|5|Briefly described|map legend|Late Devonian||||||||
17459|Stud Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
17459|Stud Formation|43095|5|Briefly described|Plate 2|||Of Dotswood Group.||||||19-FEB-07
17459|Stud Formation|43933|5|Briefly described|Map Legend||Late Devonian|Of Dotswood Group.||||||
17459|Stud Formation|62522|2|Defined|p24|Frasnian|Frasnian|Of Dotswood Group. Conformable over Vanneck Formation; unconformable over Argentine Metamorphics; conformably underlies Julia Formation. Thickness: 800m. Geological Province: Burdekin Basin.||||||13-NOV-07
17459|Stud Formation|65214|6|Mentioned|p279, p280, p283|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17459|Stud Formation|67402|4|Described|p239, p246, p247, p248|Frasnian|Frasnian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under ephemeral lake, fluvial flood-channel and alluvial plain conditions.||||Overlies the Vanneck Formation. Overlain by the Julia Formation and the Kukiandra Formation.|Micaceous mudstones and siltstones with lesser very fine-grained sandstone. Tuff, tuffaceous siltstone and conglomerate are also present.|
17459|Stud Formation|68350|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Vanneck Formation. Is overlain conformably by Julia Formation.|Red calcareous mudstone and siltstone, fine-grained red to grey feldspathic sandstone, minor algal and oolitic limestone and minor tuff and conglomerate.|
17459|Stud Formation|68351|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Vanneck Formation. Is overlain conformably by Julia Formation.|Red calcareous mudstone and siltstone, fine-grained red to grey feldspathic sandstone, minor algal and oolitic limestone and minor tuff and conglomerate.|
17459|Stud Formation|68419|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin. Includes an informal unnamed subunit.||Of the Dotswood Group.||Conformably overlain by the Julia Formation. Conformably underlain by the Vanneck Formation.|Red calcareous mudstone and siltstone, fine-grained red to grey feldspathic sandstone, minor algal and oolitic limestone and minor tuff and conglomerate; fine to coarse-grained lithofeldspathic and quartzose sandstone and greyish siltstone.|
17459|Stud Formation|68420|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin. Includes an informal unnamed subunit.||Of the Dotswood Group.||Conformably overlain by the Julia Formation. Conformably underlain by the Vanneck Formation.|Red calcareous mudstone and siltstone, fine-grained red to grey feldspathic sandstone, minor algal and oolitic limestone and minor tuff and conglomerate; fine to coarse-grained lithofeldspathic and quartzose sandstone and greyish siltstone.|
17459|Stud Formation|68731|4|Described|p177 Fig 3.91, p185 Tb 3.4, p186|Famennian|Frasnian|Burdekin Basin. Alluvial plain with extensive development of ephemeral lakes and ponds with algal carbonate generation or placoderm fish. Red weathering of the sediment source with a common pedigenic carbonate contribution. < 1000 m thick.||Of the Dotswood Group.|Includes the Yarraman Sandstone Member.||Comprises red micaceous siltstone and mudstone, commonly mudcracked, with subordinate fine to medium lithofeldspathic sandstone. Sporadic thin tuffaceous beds, coarse volcaniclastic sandstone and pebble conglomerate. Rare lacustrine limestone beds.|
17462|Sturgeon Basalt|23422|4|Described|p187, p204 Table 6.3|Quaternary|Pliocene|Geological Province: Sturgeon Subprovince.||||||
17462|Sturgeon Basalt|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
17462|Sturgeon Basalt|32553|4|Described|p34|||||||||
17462|Sturgeon Basalt|33638|5|Briefly described|Table 2|||||||||
17462|Sturgeon Basalt|33641|6|Mentioned|p60|||Cainozoic.||||||
17462|Sturgeon Basalt|33643|6|Mentioned|Map legend|Quaternary|Tertiary|Tertiary-Quaternary||||||
17462|Sturgeon Basalt|33644|6|Mentioned|Map legend|Pleistocene|Pliocene|Pliocene - Pleistocene||||||
17462|Sturgeon Basalt|33648|6|Mentioned|p24|||Strat.||||||
17462|Sturgeon Basalt|33958|6|Mentioned|p40|||See also p45.||||||06-MAY-15
17462|Sturgeon Basalt|34046|6|Mentioned|Table III|||||||||
17462|Sturgeon Basalt|36472|6|Mentioned|Map legend|Pleistocene|Pliocene|Pleistocene to Pliocene.||||||
17462|Sturgeon Basalt|39445|5|Briefly described|Table 14|||||||||
17462|Sturgeon Basalt|44353|14|Not recorded|p422|Early Pleistocene|Late Pliocene|See also Lexicon.||||||
17462|Sturgeon Basalt|44800|14|Not recorded|p22|Pleistocene|Tertiary|late Tertiary-early Pleistocene.||||||
17462|Sturgeon Basalt|45087|5|Briefly described|p165|||Chemical analyses||||||
17462|Sturgeon Basalt|45151|5|Briefly described|Table 12|||||||||
17462|Sturgeon Basalt|48903|6|Mentioned|p24|||||||||
17462|Sturgeon Basalt|64707|5|Briefly described|Map legend|Quaternary|Tertiary|Age is Tertiary to Tertiary-Quaternary. Olivine basalt||||||08-DEC-08
17462|Sturgeon Basalt|68338|5|Briefly described|Map legend.|Neogene|Neogene|Sturgeon Basalt Province.|||||Olivine basalt.|
17462|Sturgeon Basalt|68478|5|Briefly described|Map Legend|Quaternary|Neogene|Sturgeon Basalt Province. Late Tertiary - Quaternary (Neogene) age. The 2 facies are mapped separately.|||||Olivine basalt.|
17462|Sturgeon Basalt|68479|5|Briefly described|Map Legend|Neogene|Paleogene|Sturgeon Basalt Province. Late Tertiary - Quaternary (Neogene) age. The 2 facies are mapped separately.|||||Olivine basalt.|
17462|Sturgeon Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, Chudleigh, McIvor River, McLean, Piebald and Wallaroo Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
17462|Sturgeon Basalt|69599|5|Briefly described|p599-600, p651|Pleistocene|Pliocene|NE Eromanga Basin. Overlies Cenozoic sediments.||||Overlies Glendower Formation locally.||
17462|Sturgeon Basalt|71394|5|Briefly described|p1, p17|Neogene|Paleogene|Galilee Basin.|||||Dark grey aphyric and vesicular basalt.|
17462|Sturgeon Basalt|73472|6|Mentioned|p117|||[Written as Sturgeon Basalts].||||||
17477|Styx Coal Measures|23042|5|Briefly described|p62, Fig 2||Cretaceous|Underlying unit Back Creek Group (un).||||||
17477|Styx Coal Measures|23840|5|Briefly described|p447|Early Cretaceous|Early Cretaceous|Geological Province: Styx Basin.  Maximum thickness: 387m.||||||
17477|Styx Coal Measures|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
17477|Styx Coal Measures|31656|6|Mentioned|Table 2|||||||||
17477|Styx Coal Measures|31659|6|Mentioned|p76|||||||||
17477|Styx Coal Measures|31979|4|Described|Table 1|||See also Table 2, P10. L.Cret.||||||
17477|Styx Coal Measures|31983|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17477|Styx Coal Measures|33128|6|Mentioned|p60|||Cretaceous||||||
17477|Styx Coal Measures|33165|6|Mentioned|Chart|||Correlation chart only||||||
17477|Styx Coal Measures|33939|6|Mentioned|p393|||L.Cretaceous||||||
17477|Styx Coal Measures|34408|6|Mentioned|p190|||||||||
17477|Styx Coal Measures|36101|6|Mentioned|p169|||||||||
17477|Styx Coal Measures|36581|6|Mentioned|p464|||||||||
17477|Styx Coal Measures|37121|4|Described|p324|||||||||
17477|Styx Coal Measures|37565|6|Mentioned|p10|||||||||
17477|Styx Coal Measures|38067|6|Mentioned|p60|||||||||
17477|Styx Coal Measures|38081|5|Briefly described|Table 1|||||||||
17477|Styx Coal Measures|39211|5|Briefly described|p44|||Age||||||
17477|Styx Coal Measures|39212|5|Briefly described|p17|||||||||
17477|Styx Coal Measures|39445|5|Briefly described|Table 11|||||||||
17477|Styx Coal Measures|41057|6|Mentioned|p61|||||||||
17477|Styx Coal Measures|41246|6|Mentioned|Map legend|Cretaceous||||||||
17477|Styx Coal Measures|41922|4|Described|Table 1, P8|||||||||
17477|Styx Coal Measures|42187|5|Briefly described|p321|||||||||
17477|Styx Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
17477|Styx Coal Measures|42648|5|Briefly described|Fig.7 P43|||||||||
17477|Styx Coal Measures|43906|2|Defined|p330,332||Early Cretaceous|Early Cretaceous, probably Albian||||||
17477|Styx Coal Measures|43994|14|Not recorded|Map Legend|||||||||
17477|Styx Coal Measures|43998|4|Described|p4,16,map||Early Cretaceous|||||||
17477|Styx Coal Measures|44002|14|Not recorded|Map Legend||Early Cretaceous|||||||
17477|Styx Coal Measures|44082|6|Mentioned|p30,Tb.34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
17477|Styx Coal Measures|44091|14|Not recorded|p61||Cretaceous|U.L.Cretaceous.||||||
17477|Styx Coal Measures|44337|5|Briefly described|Map Legend||Cretaceous|Lithology.||||||
17477|Styx Coal Measures|44409|14|Not recorded|Map Legend||Cretaceous|||||||
17477|Styx Coal Measures|44635|4|Described|p11,map||Early Cretaceous|||||||
17477|Styx Coal Measures|44728|14|Not recorded|p222|||Overlies Apis Creek Formation.||||||
17477|Styx Coal Measures|44876|14|Not recorded|p75||Albian|||||||
17477|Styx Coal Measures|45071|4|Described|p82|||||||||
17477|Styx Coal Measures|45114|6|Mentioned|p8|||Lower Cretaceous age.||||||
17477|Styx Coal Measures|48881|14|Not recorded|Tb.1,p8||Cretaceous|||||||
17477|Styx Coal Measures|48898|6|Mentioned|p2|||L.Cret. See also PP9,31,61 etc||||||
17477|Styx Coal Measures|48915|6|Mentioned|Table 1|||Cretaceous||||||
17477|Styx Coal Measures|60479|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Quartzose sandstone, mudstone, conglomerate and coal.||||||
17477|Styx Coal Measures|60481|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Quartzose sandstone, mudstone, conglomerate and coal.||||||
17477|Styx Coal Measures|61035|5|Briefly described|p19, p70|Early Cretaceous|Early Cretaceous|Uncomformably underlain by Back Creek Group. Isolated block of sedimentary rocks. Geological Province: Styx Basin. Consists of quartzose sandstone, green lithic sandstone, mudstone, conglomerate and coal.||||||07-FEB-11
17477|Styx Coal Measures|64665|5|Briefly described|p62.|Early Cretaceous|Early Cretaceous|Styx Basin. c.1000 m thick. Small-scale mining for thermal coal took place in the mid 20th century; not currently exploited. High volatile bituminous; ash content 8.3 to 15.5%; poor coking properties.||||Unconformably overlies Back Creek Group.||
17477|Styx Coal Measures|65096|5|Briefly described|p378|||De Jersey (1960). Styx Basin, central Queensland. Coal seams distinguished on palynology.||||||
17477|Styx Coal Measures|65388|4|Described|p216-218; p217 Fig.75; p218 Fig.76|Early Cretaceous|Early Cretaceous|Of Styx Basin. Malone & others (1969) gave a summary of the geology on which this description is based. Unconformably overlie Back Creek Group.  Age from plant fossils and spores approximately Albian. Dominantly freshwater sediments (250-425m) consisting mostly of fine-grained, grey to green lithic sandstone, mudstone, conglomerate and thin coal seams.||||||
17477|Styx Coal Measures|67402|4|Described|p239, p256|Albian|Albian|Styx Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited as graben fill in a fluvial environment. 528m thick.|||||Sandstone, shale, conglomerate and coal.|
17477|Styx Coal Measures|68008|6|Mentioned|p264|||Styx Basin.||||Age-equivalent to Stanwell Formation.||
17477|Styx Coal Measures|68359|5|Briefly described|p3-4,p7,p9-10,p14-18,p21-24, App.3,8,10|Early Cretaceous|Early Cretaceous|Benstead (1976). Styx Basin. Up to 900m thick; 288.76m thickness was intersected in this drillhole. No aquifers nor natural underground reservoirs were intersected. Fluvial, coastal plain sequence. Coal has high rank and vitrinite reflectance values. Temperature log; detailed lithologies and photographs of core; thermal conductivity results; detailed lithology and geophysics log' vitrinite reflectance values; thermal profile and heat flow model.||||Overlies Back Creek Group.|Includes quartzose sandstone, siltstone, mudstone and numerous coal seams.|05-MAR-19
17477|Styx Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Styx Basin.||||||
17477|Styx Coal Measures|68679|6|Mentioned|p312-313, p347|Cretaceous|Cretaceous|Northern New England Orogen.||||||
17477|Styx Coal Measures|69582|5|Briefly described|p57-p60|Early Cretaceous|Early Cretaceous|Styx Basin. Thermal conductivity and geothermal energy potential are discussed. Intersected in GSQ St Lawrence 1.||||Overlies the Back Creek Group.|Sandstone, mudstone, coal and conglomerate with sporadic marine incursions. Numerous coal seams are present which vary in thickness and extent.|
17477|Styx Coal Measures|69594|5|Briefly described|p550, p552|Early Cretaceous|Early Cretaceous|Dunstan in Walkom (1919). The constituent unit in the Styx Basin. Up to 529m onshore; ~900m offshore. Freshwater deltaic to paludal deposits with sporadic marine incursions. Coal mining started in 1919; very low gas flows; CSG exploration is continuing; unsuitable for carbon sequestration.||||Onlaps the Back Creek Group. Correlated with Coreena Member (Wallumbilla Formation), Griman Creek Formation, Burrum and Stanwell Coal Measures, and (partly) Jim Crow beds.|Mainly fine to medium, quartzose, feldspathic and lithic sandstones, mudstones, siltstones, carbonaceous shales, coal; minor pebbly conglomerate. Primary volcanics are absent, but significant portions of coarser clastics may be volcanilithic.|
17477|Styx Coal Measures|72297|5|Briefly described|p700, p751|Early Cretaceous|Early Cretaceous|Styx Basin. ~1000m thick; 14m of net coal. State collieries closed in 1963 when diesel locomotives replaced steam. Encouraging results from CSG exploration.||||Unconformably overlies the Back Creek Group.|Coal seams up to 1m thick.|
17500|Sugarloaf Metamorphics|23440|5|Briefly described|p139|||||||||
17500|Sugarloaf Metamorphics|23799|3|Fully described|p20, p15 Tb. 1|Carboniferous|Devonian|Intruded by Woolshed Mountain Granodiorite, and units of Eskdale Granodiorite, Crows Nest Granite, Djuan Tonalite and Boondooma Igneous Complex. Geological Province: Yarraman Subprovince (Wandilla Province).  See also p123.||||||09-APR-08
17500|Sugarloaf Metamorphics|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
17500|Sugarloaf Metamorphics|24560|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
17500|Sugarloaf Metamorphics|30303|6|Mentioned|p322|||Relationship to Cranbrook Group not known.||||||27-OCT-08
17500|Sugarloaf Metamorphics|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
17500|Sugarloaf Metamorphics|32912|5|Briefly described|p157|||Contacts and intrusions.||||||09-APR-08
17500|Sugarloaf Metamorphics|35101|4|Described|p16|||||||||
17500|Sugarloaf Metamorphics|37252|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian-Carboniferous||||||
17500|Sugarloaf Metamorphics|37376|6|Mentioned|Table 1|||||||||
17500|Sugarloaf Metamorphics|39445|5|Briefly described|Table 6|||See also p83.||||||09-APR-08
17500|Sugarloaf Metamorphics|41917|6|Mentioned|Fig.3 P528|||||||||
17500|Sugarloaf Metamorphics|42525|5|Briefly described|Map legend|Paleozoic|Paleozoic|Geological Province: Yarraman Block.||||||07-NOV-08
17500|Sugarloaf Metamorphics|42547|5|Briefly described|p54|||||||||
17500|Sugarloaf Metamorphics|43008|5|Briefly described|map legend|||||||||
17500|Sugarloaf Metamorphics|43009|5|Briefly described|Map Legend|||||||||
17500|Sugarloaf Metamorphics|50384|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince.||||||
17500|Sugarloaf Metamorphics|60077|5|Briefly described|Map legend|Paleozoic|Paleozoic|Slate, mica-schist.||||||07-NOV-08
17500|Sugarloaf Metamorphics|60370|5|Briefly described|Map Legend|Carboniferous|Devonian|Geological Province: Yarraman Subprovince. Slate, spotted slate, phyllite, quartzite, schist, amphibolite||||||02-SEP-04
17500|Sugarloaf Metamorphics|61781|6|Mentioned|p267|||Geological Province: Yarraman Block.||||||
17500|Sugarloaf Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Yarraman Subprovince. This unit, as well as Bjelke Petersen and Maronghi Creek beds, Fifer Creek and Mountefontein Metamorphics, and unnamed sedimentary units, are all mapped under the symbol, DCym.||||||
17500|Sugarloaf Metamorphics|68679|5|Briefly described|p321-323, p413-414|Late Carboniferous|Late Carboniferous|Campbell (1952). Up to 15km wide. Yarraman Subprovince, Wandilla Province, northern New England Orogen. Lower plate component of an extensional complex. Age unknown, but predates a Permian intrusion. RELATED UNITS (continued): Is faulted against the Maronghi Creek beds and Cressbrook Creek Group.||||Is overlain unconformably by Tarong beds and Main Range Volcanics. Intruded by Woolshed Mountain, Eskdale Granodiorites, Crows Nest Granite, Djuan Tonalite, Boondooma Igneous Complex. See COMMENTS.|Variably bedded, fine-grained sandstone; some black slate, shale, phyllite and quartz-mica schist. Spotted hornfels adjacent to granitoids; abundant quartz veins common in pelitic rocks. Has a distinct unit of schistose amphibolite and metavolcanics.|
17504|Sugars Basalt|30302|6|Mentioned|p414|||Refers to Allen(1959)||||||
17504|Sugars Basalt|33381|5|Briefly described|p113|||Triassic||||||
17504|Sugars Basalt|35161|6|Mentioned|p591|||||||||
17504|Sugars Basalt|35866|6|Mentioned|p402|||||||||
17504|Sugars Basalt|36779|6|Mentioned|p6|||||||||
17504|Sugars Basalt|36954|6|Mentioned|Fig.1|||||||||
17504|Sugars Basalt|38074|5|Briefly described|Table 1|||||||||
17504|Sugars Basalt|38307|6|Mentioned|p523|||||||||
17504|Sugars Basalt|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
17504|Sugars Basalt|39445|6|Mentioned|Table 9|||||||||
17504|Sugars Basalt|40623|5|Briefly described|p30|||Mention Table 2||||||
17504|Sugars Basalt|41591|5|Briefly described|p21|||||||||
17504|Sugars Basalt|41906|3|Fully described|Table 2 P19|||||||||
17504|Sugars Basalt|42893|5|Briefly described|p6|||of Kholo Subgroup||||||
17504|Sugars Basalt|43076|6|Mentioned|p5|||||||||
17504|Sugars Basalt|43150|5|Briefly described|Map Legend||Triassic|Of the Ipswich Coal Measures. Geological Province: Ipswich Basin.||||||12-APR-05
17504|Sugars Basalt|44510|14|Not recorded|Fig.35|||||||||
17504|Sugars Basalt|44542|2|Defined|p32,33||Middle Triassic|Overlain by sediments of Kholo Sub-Group. Probably equivalent to Weir Basalt.||||||
17504|Sugars Basalt|44687|6|Mentioned|p227|||Disconformably overlain by Witty Gravel.||||||21-MAR-13
17504|Sugars Basalt|44703|14|Not recorded|Map|||Spilitic volcanics.||||||
17504|Sugars Basalt|44705|14|Not recorded|1-4,7-10,15,16|||||||||
17504|Sugars Basalt|44707|14|Not recorded|p3|||||||||
17504|Sugars Basalt|44708|14|Not recorded|p3,Sheet 2||Middle Triassic|||||||
17504|Sugars Basalt|44775|14|Not recorded|Map 2||Middle Triassic|||||||
17504|Sugars Basalt|44783|14|Not recorded|p18|||||||||
17504|Sugars Basalt|45087|5|Briefly described|p154|||Chemical analyses||||||
17504|Sugars Basalt|68679|4|Described|p393-394, p435|Late Triassic|Late Triassic|Ipswich Basin. 37m thick in the type section and ~100m thick in drill holes. Geochronology by Webb and McNaughton (1978).|232 Ma and 229 Ma (K-Ar whole rock).|Kholo Subgroup.||Is overlain by Mount Crosby Formation. Upper part is equivalent to Weir Basalt.|At least nine individual, thin lava flows: basalt to basaltic andesite lavas from aphyric to moderately porphyritic, and from massive to highly amygdaloidal. Airfall tuffs and possible pillow lavas suggest water interaction.|
17504|Sugars Basalt|73306|5|Briefly described|p565-566, 573|Late Triassic|Late Triassic|Base of the Ipswich Basin. May represent the initial stage of rifting.|c.232-229 Ma (Purdy and Cross, 2013).|||||
17504|Sugars Basalt|73450|5|Briefly described|p38|Carnian|Carnian|Whole-rock K-Ar ages of 229 Ma and 232 Ma were reported by Webb and McNaughton (1978).|229 Ma, 232 Ma; whole-rock K-Ar||||Multiple, thin aphanitic to moderately porphyritic and massive to highly amygdaloidal lava flows.|
17519|Sun Hill Arkose|10116|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Arkose, feldspathic sandstone, micaceous sandstone, siltstone, arkosic conglomerates.||||||
17519|Sun Hill Arkose|22954|6|Mentioned|Fig3p9|||||||||
17519|Sun Hill Arkose|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
17519|Sun Hill Arkose|31287|5|Briefly described|p430|||Refers to status||||||
17519|Sun Hill Arkose|33111|4|Described|p43|||Mention p18.||||||05-DEC-06
17519|Sun Hill Arkose|34454|6|Mentioned|p10|||L.Cambrian||||||
17519|Sun Hill Arkose|34847|6|Mentioned|p31|||||||||
17519|Sun Hill Arkose|35121|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17519|Sun Hill Arkose|35139|4|Described|Table.2|||||||||
17519|Sun Hill Arkose|36234|3|Fully described|p166|||||||||
17519|Sun Hill Arkose|36243|6|Mentioned|Table 1A|||||||||
17519|Sun Hill Arkose|37572|6|Mentioned|p155|||See also Fig.8||||||
17519|Sun Hill Arkose|39445|5|Briefly described|Table 4|||See also p62 and Fig.5.||||||05-DEC-06
17519|Sun Hill Arkose|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
17519|Sun Hill Arkose|42060|6|Mentioned|Fig.5 P140|||||||||
17519|Sun Hill Arkose|42956|5|Briefly described|p27|||||||||
17519|Sun Hill Arkose|44121|14|Not recorded|p5|Early Cambrian|Neoproterozoic|||||||
17519|Sun Hill Arkose|44211|14|Not recorded|p95,97,102,104|||||||||
17519|Sun Hill Arkose|44291|14|Not recorded|p8|||||||||
17519|Sun Hill Arkose|44308|14|Not recorded|p3,5,13,Tb.1||Cambrian|Equivalent to Mount Birnie Beds.||||||
17519|Sun Hill Arkose|44310|14|Not recorded|Map Legend||Early Cambrian|||||||
17519|Sun Hill Arkose|44312|14|Not recorded|Map Legend||Early Cambrian|||||||
17519|Sun Hill Arkose|44543|2|Defined|p31,36||Early Cambrian|Equivalent to Mount Birnie Beds.||||||
17519|Sun Hill Arkose|44920|14|Not recorded|Map Legend, Sheet 4||Adelaidean|||||||
17519|Sun Hill Arkose|44989|14|Not recorded|p.122|||||||||
17519|Sun Hill Arkose|45002|14|Not recorded|p16|||Early Late Cambrian fossils present.||||||05-DEC-06
17519|Sun Hill Arkose|45012|14|Not recorded|p29||Early Cambrian|||||||
17519|Sun Hill Arkose|45052|3|Fully described|p75|||Adelaidean ?||||||
17519|Sun Hill Arkose|45102|6|Mentioned|p43|||||||||
17519|Sun Hill Arkose|48906|14|Not recorded|Tb.1|||||||||
17519|Sun Hill Arkose|49027|5|Briefly described|p3|||||||||
17519|Sun Hill Arkose|60122|6|Mentioned|p9|||||||||
17519|Sun Hill Arkose|63450|5|Briefly described|p78 Fig. 5, p80|Neoproterozoic|Neoproterozoic|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
17519|Sun Hill Arkose|64068|3|Fully described|p45-46, p54, p viii|Cryogenian||Basal glacial outwash. Is overlain by Sylvester Sandstone. Correlated with Black Stump Arkose on lithologic similarity. Also correlated with Wonnadinna Dolostone, Oorabra Arkose, Boko, Olympic Formations, Pioneer Sandstone, Mount Doreen Formation.||Of Keepera Group.||Is overlain by Sylvester Sandstone.|Arkose, arkosic sandstone, green shale, micaceous greywacke, siltstone, dolomitic siltstone, pebble conglomerate and arkosic dolostone. Basal glacial outwash.|04-APR-12
17519|Sun Hill Arkose|65338|6|Mentioned|p60.|||||Unit in Keepera Group.||||
17519|Sun Hill Arkose|65489|5|Briefly described|p125|Cambrian|Proterozoic|Georgina Basin.||||Overlies Field River Beds. Is overlain by Mount Binnie Beds and Sylvester Sandstone.||
17519|Sun Hill Arkose|67323|5|Briefly described|GIS attrib tbl, p92 Fig.12.2|Early Cambrian|Neoproterozoic|See also Solid Geology Map. Centralian Superbasin||||is overlain by Marqua Formation.|Conglomerate, arenite, arkose, shale, mudstone, dolomite|
17519|Sun Hill Arkose|67402|6|Mentioned|p215 fig GRG8/GRG9|||||||||
17519|Sun Hill Arkose|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
17519|Sun Hill Arkose|68270|4|Described|p681-683,686,688|Cryogenian|Cryogenian|Southern Georgina Basin.Type section occurs at Sun Hill and low hills to N, 19km SE of Glenormiston Homestead; lat 23'1.9'S, long. 138'52"E. Less than 300m thick. Glacial outwash deposit related to Elatina glaciation. Correlative to Elatina Formation. Laterally equivalent to Oorabra Arkose and Black Stump Arkose.||||Overlain unconformably by Sylvester Sandstone.|Arkose, arkosic sandstone, shale, siltstone, dolomitic siltstone, conglomerate and arkosic dolomite.|03-JUL-19
17519|Sun Hill Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump and Gnallan-a-gea Arkoses, Yardida and Little Burke Tillites, are all mapped under the symbol, -P-Cg.||||||
17519|Sun Hill Arkose|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Centralian A Superbasin. Supersequence 3.||Keepera Group.|||Glacial outwash deposits.|12-JUL-16
17519|Sun Hill Arkose|69443|5|Briefly described|p28:7-8|Cryogenian|Cryogenian|Georgina Basin.||Keepera Group.||||12-JUL-16
17519|Sun Hill Arkose|69591|5|Briefly described|p94|||E of Toko Syncline in the Sylvester Creek drainage. Has a complicated history of interpretation (detailed) by various workers.||||Is overlain by Sylvester Sandstone.|Arkosic sandstone, conglomerate, siltstone and dolomite.|
17519|Sun Hill Arkose|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Georgina Basin.||||Equivalent to the Oorabra Arkose.||02-JUN-21
17522|Sunburst Granodiorite|22847|3|Fully described|p 43|Early Ordovician||||||||
17522|Sunburst Granodiorite|23422|5|Briefly described|p173, p210 Table 6.6|Ordovician|Ordovician|Of Sunburst Suite. Age: 482+/-8Ma.||||||
17522|Sunburst Granodiorite|23430|4|Described|p480|||SHRIMP Pb/U 482 +/- 8 Ma. Ravenswood Batholith Province.||||||
17522|Sunburst Granodiorite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 464. I-Type.||||||
17522|Sunburst Granodiorite|42633|5|Briefly described|Table 1 P11|||Variation on Sunburst Quartz Diorite?||||||
17522|Sunburst Granodiorite|42750|2|Defined|p33|Early Ordovician|Late Cambrian|||||||
17522|Sunburst Granodiorite|43093|4|Described|Appendix 1|||possible Late Cambrian to Early Ordovician||||||
17522|Sunburst Granodiorite|43259|4|Described|Appendix 1,p49.|Early Ordovician|Late Cambrian|||||||
17522|Sunburst Granodiorite|43934|5|Briefly described|Map Legend||Ordovician|||||||
17522|Sunburst Granodiorite|50552|5|Briefly described|p1048 Fig.2|Late Ordovician|Early Ordovician|In Lolworth-Ravenswood Terrane.||||||24-NOV-04
17522|Sunburst Granodiorite|62074|6|Mentioned|p2|Early Ordovician|Late Cambrian|Charters Towers area.||||||
17522|Sunburst Granodiorite|62075|6|Mentioned|p11 Fig.3|Middle Ordovician|Early Ordovician|Appears as Sunburst granodiorite.||||||
17522|Sunburst Granodiorite|62521|5|Briefly described|p26, p30|||Of the Sunburst Suite. Geological Province: Ravenswood Batholith.||||||21-DEC-07
17522|Sunburst Granodiorite|68576|6|Mentioned|Q_11: p42|||Charters Towers.||||||
17522|Sunburst Granodiorite|68731|5|Briefly described|p146, p147, p150|Early Ordovician|Furongian|Peters (1987) suggested a mantle source for the Sunburst Granodiorite. U/Pb SHRIMP geochronology by Hutton et al. (1994).|482 +/- 8 Ma||||Comprises a melanocratic hornblende-biotite granodiorite to tonalite.|12-MAY-16
17522|Sunburst Granodiorite|71592|5|Briefly described|Appendix A.|||Macrossan Igneous Province, Thomson Orogen.|482+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
17527|Sunday Creek Volcanics|23423|5|Briefly described|p237|||Included in the Glen Gordon Volcanics||||||
17527|Sunday Creek Volcanics|23494|5|Briefly described|p10, p20 Tb. 1|Permian|Carboniferous|Mainly altered rhyolite and ignimbrite, some andesite.  Intruded by Herbert River Granite.  Max. thickness: 400ft.||||||
17527|Sunday Creek Volcanics|23497|6|Mentioned|p30|||Superseded into Glen Gordon Volcanics.||||||
17527|Sunday Creek Volcanics|23616|6|Mentioned|Table 3 p45|||Of Best 1962 and Branch 1966.  Included in Glen Gordon Volcanics.||||||
17527|Sunday Creek Volcanics|23619|5|Briefly described|p9|||In Einasleigh Sheet area rocks assigned to Glen Gordon Volcanics probably current outside this area.||||||
17527|Sunday Creek Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17527|Sunday Creek Volcanics|31832|6|Mentioned|Table 6|||||||||
17527|Sunday Creek Volcanics|32553|4|Described|p46|||||||||
17527|Sunday Creek Volcanics|37613|6|Mentioned|p252|||||||||
17527|Sunday Creek Volcanics|39027|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
17527|Sunday Creek Volcanics|39445|5|Briefly described|Table 7|||||||||
17527|Sunday Creek Volcanics|43113|6|Mentioned|p9|||||||||
17527|Sunday Creek Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
17527|Sunday Creek Volcanics|43927|14|Not recorded|p12|||||||||
17527|Sunday Creek Volcanics|44048|14|Not recorded|Map Legend||Carboniferous|||||||
17527|Sunday Creek Volcanics|44296|14|Not recorded|Map Legend||Carboniferous|||||||
17527|Sunday Creek Volcanics|45009|14|Not recorded|p75,Tb.13,Pl.13|||Rhyolite.||||||
17527|Sunday Creek Volcanics|45014|2|Defined|p47-51,62,65,103,||Early Carboniferous|Pl.38,Tb.1. (Probably Middle Carboniferous)||||||
17527|Sunday Creek Volcanics|45025|4|Described|p67|Permian|Carboniferous|||||||
17527|Sunday Creek Volcanics|45065|6|Mentioned|p27|||||||||
17527|Sunday Creek Volcanics|45113|6|Mentioned|p26|||||||||
17527|Sunday Creek Volcanics|46845|6|Mentioned|Table 1|||||||||
17534|Sunny Park Granodiorite|42747|5|Briefly described|Fig.9, Table 1|||same as Sunny Park Granite||||||
17534|Sunny Park Granodiorite|43029|2|Defined|p14||Devonian|see also Fig.2,p16||||||
17534|Sunny Park Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
17534|Sunny Park Granodiorite|43213|3|Fully described|p35, p96-97, p102, p116-121, p170, p175|Devonian|Devonian|See also p179, p209, p223-224, p231, p240. Part of Retreat Batholith, on the NNW margin. Type area described. Similar to Kilmarnock Granodiorite. Geochemistry, modal and chemical analyses and geophysics detailed. Strongly magnetic.||||Intrudes Rolfe Creek Schist. Is faulted against Theresa Creek Volcanics. Is overlain unconformably by Silver Hills Volcanics.|Grey, fine- to medium-grained, equigranular hornblende-biotite granodiorite to granite with subordinate pink, porphyritic microgranite.|
17534|Sunny Park Granodiorite|43861|5|Briefly described|29||Devonian|Intrudes Rolfe Creek Schist||||||
17534|Sunny Park Granodiorite|68412|5|Briefly described|Map legend|Late Devonian|Middle Devonian||||||Grey, fine- to medium-grained, hornblende-biotite granodiorite and subordinate pink, porphyritic microgranite.|
17534|Sunny Park Granodiorite|68482|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey, fine to medium-grained, hornblende-biotite granodiorite and subordinate pink, porphyritic microgranite.|
17537|Sunnybank Formation|31273|6|Mentioned|p3|||||||||
17537|Sunnybank Formation|38074|5|Briefly described|Table 1|||||||||
17537|Sunnybank Formation|39445|5|Briefly described|Table 14|||See also P150. Middle Tertiary||||||
17537|Sunnybank Formation|40623|5|Briefly described|p8|||See also P109||||||
17537|Sunnybank Formation|44581|14|Not recorded|p349|||Overlies Darra Formation.||||||
17537|Sunnybank Formation|44677|14|Not recorded|p1|||||||||
17537|Sunnybank Formation|44687|1|Redefined|p224,226|||Formation of Oxley Group.||||||
17537|Sunnybank Formation|44703|14|Not recorded|Map||Tertiary|||||||
17537|Sunnybank Formation|44708|14|Not recorded|p3,section,Sh.1-3||Tertiary|||||||
17537|Sunnybank Formation|44783|14|Not recorded|p2,Tb.1||Oligocene|||||||
17537|Sunnybank Formation|61155|5|Briefly described|p19|Middle Eocene|Middle Eocene|Of the Oxley Group. Overlies the Corinda Formation. Age: 46-40.5Ma. Thickness: 30m. In the Brisbane region.||||||
17537|Sunnybank Formation|69599|5|Briefly described|p586, p594-595|Miocene|Eocene|McTaggart (1960); Houston (1965). Oxley Basin. Up to 164m thick. Fluvial to lacustrine deposits. Fossils include vertebrates, bivalves, plants and crustaceans. Capped by laterite.||Oxley Group.||Disconformably overlies Corinda Formation.|Claystone, sandstone, conglomerate and limestone.|
17546|Surat Siltstone|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3, p498|Albian|Albian|N Surat Basin. 100-130m thick.||||Overlies Coreena Member (Wallumbilla Formation).|Interbedded siltstone (commonly micaceous) and mudstone (generally carbonaceous and pyritic) with lenses of fine-grained glauconitic sandstone; small pelecypods common.|
17546|Surat Siltstone|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||?Of Rolling Downs Group||||
17546|Surat Siltstone|22757|5|Briefly described|Table6,p11||Early Cretaceous|150 m thick. Surat Basin.||||||21-APR-09
17546|Surat Siltstone|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig. 22.8|Albian|Albian|Of the Rolling Downs Group. Basal mudstone overlain by thinly bedded siltstone. Equivalent to Surat Siltstone (Wallumbilla Formation) in Eromanga Basin. Max. thickness: ~220m. Geol. Province: Surat Basin. See also p312-3 Fig.22.6, p544 App.1 Tb.A1.12.||||||
17546|Surat Siltstone|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
17546|Surat Siltstone|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||13-MAR-09
17546|Surat Siltstone|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Basin: Surat Basin.||||||
17546|Surat Siltstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
17546|Surat Siltstone|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 110m.||||||
17546|Surat Siltstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
17546|Surat Siltstone|29387|6|Mentioned|Table 5|||||||||
17546|Surat Siltstone|29721|6|Mentioned|Table 246|||||||||
17546|Surat Siltstone|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
17546|Surat Siltstone|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
17546|Surat Siltstone|31116|4|Described|p44|||See also Table 2. Cretaceous.||||||
17546|Surat Siltstone|31208|6|Mentioned|Table 1|||See also Fig. 3 & 567. Early Albian||||||
17546|Surat Siltstone|31376|6|Mentioned|p4|||||||||
17546|Surat Siltstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|32314|6|Mentioned|Fig. 4|||||||||
17546|Surat Siltstone|32796|2|Defined|p301|middle Albian|early Albian|Lower-Middle Albian||||||
17546|Surat Siltstone|33016|6|Mentioned|p25|||||||||
17546|Surat Siltstone|33070|4|Described|Table 2|||L.Cret.||||||
17546|Surat Siltstone|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|33090|4|Described|Table 4|||L.Cret.||||||
17546|Surat Siltstone|33091|5|Briefly described|p9|||Strat.||||||
17546|Surat Siltstone|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|33448|6|Mentioned|p7|||||||||
17546|Surat Siltstone|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|34613|4|Described|Table 4|||||||||
17546|Surat Siltstone|35793|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
17546|Surat Siltstone|35937|6|Mentioned|Fig.5|||||||||
17546|Surat Siltstone|36243|6|Mentioned|Table 7A|||||||||
17546|Surat Siltstone|36581|6|Mentioned|p464|||||||||
17546|Surat Siltstone|37117|5|Briefly described|p313|||||||||
17546|Surat Siltstone|37995|4|Described|p66|||||||||
17546|Surat Siltstone|39211|5|Briefly described|Fig.21|||||||||
17546|Surat Siltstone|39212|5|Briefly described|p18|||||||||
17546|Surat Siltstone|39445|5|Briefly described|Table 11|||||||||
17546|Surat Siltstone|39943|6|Mentioned|Table 9B|||||||||
17546|Surat Siltstone|40245|6|Mentioned|Table 2|||||||||
17546|Surat Siltstone|40249|6|Mentioned|p38|||||||||
17546|Surat Siltstone|40801|6|Mentioned|p65|||||||||
17546|Surat Siltstone|41060|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|41064|6|Mentioned|p62|||||||||
17546|Surat Siltstone|41187|6|Mentioned|Fig.2|||||||||
17546|Surat Siltstone|41216|6|Mentioned|Fig.18|||||||||
17546|Surat Siltstone|41266|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|41992|4|Described|Fig.2 P183|||||||||
17546|Surat Siltstone|42007|5|Briefly described|Fig.2 P182|||||||||
17546|Surat Siltstone|42429|5|Briefly described|p155|||||||||
17546|Surat Siltstone|42494|5|Briefly described|Table 1 P24|||||||||
17546|Surat Siltstone|42673|5|Briefly described|Fig.2, P184|||||||||
17546|Surat Siltstone|43000|5|Briefly described|Fig.5,p112|||Of Rolling Downs Group.||||||13-MAR-09
17546|Surat Siltstone|43002|5|Briefly described|Fig.2,p135|||||||||
17546|Surat Siltstone|43602|5|Briefly described|Fig3 p194|||In Surat Basin, Rolling Downs Group.||||||21-APR-09
17546|Surat Siltstone|45110|2|Defined|p120|middle Albian|middle Albian|See also P24.||||||
17546|Surat Siltstone|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
17546|Surat Siltstone|46791|4|Described|p47|||||||||
17546|Surat Siltstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
17546|Surat Siltstone|46984|6|Mentioned|Table 1|||||||||
17546|Surat Siltstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
17546|Surat Siltstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
17546|Surat Siltstone|60524|5|Briefly described|p488|Albian|Albian|Marine unit.  Geological Province: Surat Basin.||||||
17546|Surat Siltstone|61221|6|Mentioned|p1||Cretaceous|Geological Province: Surat Basin.||||||
17546|Surat Siltstone|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Siltstone, mudstone. Geological Province: Surat Basin.||||||07-FEB-11
17546|Surat Siltstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
17546|Surat Siltstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|Surat Basin||||Underlies Griman Creek Formation; overlies Wallumbilla Formation.||
17546|Surat Siltstone|64856|3|Fully described|p79, p100-102|Albian|Albian|Surat Basin only. Of Reiser (1970). Implied type section is the interval 15-140m in GSQ Surat 1. Fine-grained sediments and sandstone. Conformably overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation. 100-130m thick. Associated with palynofloral units APK4 and 51. Contains dinoflagellate assemblages conformable with units ADK19, 21.|| ||||29-NOV-17
17546|Surat Siltstone|64857|5|Briefly described|p113 Fig.3|||Overlies Wallumbilla Formation, Surat Basin.||||||
17546|Surat Siltstone|64858|6|Mentioned|p187-188|||See also Surat Formation.||||||30-NOV-09
17546|Surat Siltstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin. Underlies the Griman Creek Formation; overlies the Coreena Member of the Wallumbilla Formation.||||||22-MAR-12
17546|Surat Siltstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Coreena Member and Wallumbilla Formation, underlies the Griman Creek Formation.||||||
17546|Surat Siltstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
17546|Surat Siltstone|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Griman Creek Formation, Overlies both the Coreena Member and Wallumbilla Formation, Surat Basin.||||||
17546|Surat Siltstone|65119|6|Mentioned|Fig 6 p512, Fig 14 p521|Early Cretaceous|Early Cretaceous|Includes siltstone, mudstone and sandstone. Present in the Cabawin 1 well. See also variation Surat Sandstone p503.||||||07-MAR-12
17546|Surat Siltstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|66623|6|Mentioned|p258, p262.|||Surat Basin. Partly equivalent to Coreena Member.||||||
17546|Surat Siltstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
17546|Surat Siltstone|67402|4|Described|p146 fig SRT3, p148, p156|Albian|Albian|Surat Basin. Deposited in shallow marine or coastal swamp environments. Approximately 125m thick.||||Overlies the Wallumbilla Formation. Overlain by the Griman Creek Formation.|Interbedded carbonaceous siltstone and mudstone.|
17546|Surat Siltstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group||Conformably overlies Wallumbilla Formation. Is conformably overlain by Griman Creek Formation.|Interbedded siltstone and carbonaceous and pyritic mudstone.|22-NOV-13
17546|Surat Siltstone|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
17546|Surat Siltstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|68593|5|Briefly described|p4, p6, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.||Rolling Downs Group.||Overlies Wallumbulla Formation. Is overlain conformably by Griman Creek Formation.|Interbedded siltstone and carbonaceous and pyritic mudstone.|
17546|Surat Siltstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Surat Basin. Shallow marine.||Of the Rolling Downs Group.||||
17546|Surat Siltstone|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent in age to the Toolebuc Formation.||Of the Rolling Downs Group.||Overlain by the Griman Creek Siltstone.||
17546|Surat Siltstone|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Wallumbilla Formation. Overlain by the Griman Creek Formation.||
17546|Surat Siltstone|69594|5|Briefly described|p519, p538-539, p574|Albian|Albian|Reiser (1970). Entirely restricted to the Surat Basin. Generally 100-130m thick. Shallow-marine, intertidal, protected bay deposits; coastal swamps in the east.||||Conformably overlies Coreena Member (Wallumbilla Formation). Is overlain conformably by Griman Creek Formation.|Dominated by interbedded carbonaceous siltstones and mudstones with labile sandstone lenses. Mudstone dominates the lowest one-fifth of the Formation but in the east, lithic sandstones dominate throughout.|
17546|Surat Siltstone|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|70821|5|Briefly described|p21 Fig 2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||Rolling Downs Group.||Overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation.||14-DEC-16
17546|Surat Siltstone|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin. Albian.||||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||||Overlies Coreena Member (Wallumbilla FZ). Is overlain by Griman Creek FZ.||
17546|Surat Siltstone|73113|6|Mentioned|p22|Late Cretaceous|Late Cretaceous|Partial aquifer.||||||
17551|Surprise Creek Formation|22438|4|Described|p537, Fig.3 p537|||||||||
17551|Surprise Creek Formation|22457|6|Mentioned|Fig29 P30|||||||||
17551|Surprise Creek Formation|22498|6|Mentioned|Fig2 P235, Fig5|||||||||
17551|Surprise Creek Formation|22585|6|Mentioned|Fig1 P736, Fig3|||Actually spelt Surprise Creek Fm.||||||
17551|Surprise Creek Formation|22680|6|Mentioned|83,85|||||||||
17551|Surprise Creek Formation|23073|5|Briefly described|p744 (fig 2), p748|||||||||
17551|Surprise Creek Formation|23393|4|Described|p19, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Sub-province. See also p17 Fig. 5.||||||24-FEB-10
17551|Surprise Creek Formation|23395|6|Mentioned|p383|||||||||
17551|Surprise Creek Formation|23396|5|Briefly described|p407 Fig.2|||||||||
17551|Surprise Creek Formation|23397|5|Briefly described|p467 Fig.2|||||||||
17551|Surprise Creek Formation|23399|4|Described|p490|||||||||
17551|Surprise Creek Formation|23406|5|Briefly described|p603|||Geological province: Lawn Hill Platform.||||||16-JUN-09
17551|Surprise Creek Formation|23408|4|Described|p511, p513 Fig. 2, p514|||Not included by Hutton et al (1981) in their McNamara Group.||||||15-JUN-09
17551|Surprise Creek Formation|23466|5|Briefly described|p267|||||||||
17551|Surprise Creek Formation|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1956 Fig.2 and p1957 Fig.3.||||||
17551|Surprise Creek Formation|23965|5|Briefly described|p1297|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier.||||||07-NOV-08
17551|Surprise Creek Formation|24048|5|Briefly described|p38|||Geological Province: Mt. Isa Inlier.||||||
17551|Surprise Creek Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17551|Surprise Creek Formation|24419|5|Briefly described|p16, p17, p13 Fig.5, p15 Fig.6|Paleoproterozoic|Paleoproterozoic|Correlates with Torpedo Creek Formation. Part of the Prize Supersequence. Western Fold Belt, Leichhardt River Subprovince; Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
17551|Surprise Creek Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlain by Torpedo Creek Quartzite and Cromwell metabasalt.||||||
17551|Surprise Creek Formation|35286|6|Mentioned|Fig.17|||||||||
17551|Surprise Creek Formation|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|36548|6|Mentioned|Fig.3|||||||||
17551|Surprise Creek Formation|37459|6|Mentioned|p426|||||||||
17551|Surprise Creek Formation|37462|4|Described|Table4.VII|||||||||
17551|Surprise Creek Formation|37568|5|Briefly described|p84|||||||||
17551|Surprise Creek Formation|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|37862|6|Mentioned|p583|||||||||
17551|Surprise Creek Formation|38232|6|Mentioned|p82|||||||||
17551|Surprise Creek Formation|38234|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|38235|6|Mentioned|p115|||||||||
17551|Surprise Creek Formation|38237|4|Described|p126|||||||||
17551|Surprise Creek Formation|38276|6|Mentioned|Fig.1|||||||||
17551|Surprise Creek Formation|38348|6|Mentioned|p7|||||||||
17551|Surprise Creek Formation|38350|4|Described|p14|||||||||
17551|Surprise Creek Formation|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17551|Surprise Creek Formation|38833|6|Mentioned|p161|||||||||
17551|Surprise Creek Formation|38835|6|Mentioned|p164|||||||||
17551|Surprise Creek Formation|38836|6|Mentioned|p165|||||||||
17551|Surprise Creek Formation|38900|6|Mentioned|p55|||||||||
17551|Surprise Creek Formation|38919|6|Mentioned|p494|||||||||
17551|Surprise Creek Formation|39202|6|Mentioned|Fig.3|||||||||
17551|Surprise Creek Formation|39362|6|Mentioned|p1468|||||||||
17551|Surprise Creek Formation|39445|5|Briefly described|Table 2|||See also p36 and p41.||||||05-DEC-06
17551|Surprise Creek Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Underlies the Torpedo Creek Quartzite.||||||15-JUN-06
17551|Surprise Creek Formation|39622|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
17551|Surprise Creek Formation|39925|6|Mentioned|p335|||See also p329.||||||05-DEC-06
17551|Surprise Creek Formation|39944|6|Mentioned|Fig.5|||||||||
17551|Surprise Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17551|Surprise Creek Formation|40221|3|Fully described|p12|||||||||
17551|Surprise Creek Formation|40623|5|Briefly described|p98|||||||||
17551|Surprise Creek Formation|40840|6|Mentioned|Map legend|||||||||
17551|Surprise Creek Formation|41248|6|Mentioned|Fig.2|||||||||
17551|Surprise Creek Formation|41277|6|Mentioned|Fig.5|||||||||
17551|Surprise Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
17551|Surprise Creek Formation|41307|4|Described|p14|||||||||
17551|Surprise Creek Formation|41791|6|Mentioned|p272|||||||||
17551|Surprise Creek Formation|41978|6|Mentioned|p494|||||||||
17551|Surprise Creek Formation|41979|6|Mentioned|Fig.2 P512|||||||||
17551|Surprise Creek Formation|42234|6|Mentioned|Fig.2 P1055|||||||||
17551|Surprise Creek Formation|42503|5|Briefly described|Fig.1 P334|||||||||
17551|Surprise Creek Formation|42565|5|Briefly described|Table 1 P5, P4|||||||||
17551|Surprise Creek Formation|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Sandstone, siltstone, shale.||||||09-FEB-09
17551|Surprise Creek Formation|42818|5|Briefly described|Fig.2 P205|||||||||
17551|Surprise Creek Formation|43235|6|Mentioned|p9|||Proterozoic.||||||
17551|Surprise Creek Formation|43608|6|Mentioned|Fig.11,p11|||||||||
17551|Surprise Creek Formation|43616|6|Mentioned|p3|||||||||
17551|Surprise Creek Formation|45161|5|Briefly described|p27|||||||||
17551|Surprise Creek Formation|45166|5|Briefly described|p14|||||||||
17551|Surprise Creek Formation|46960|2|Defined|p222|Proterozoic|Proterozoic|||||||
17551|Surprise Creek Formation|46962|4|Described|Table 1|||See also Fig.3.||||||
17551|Surprise Creek Formation|47083|3|Fully described|p12-13||Proterozoic|Previously mapped as 'Surprise Creek Beds' and 'Ploughed Mountain Beds'. Informally divided into 4 units. Overlain by McNamara and Mt Isa Groups. Underlain by Bigie Formation, Fiery Creek Volcanics, Quilalar Formation and Myally Subgroup.||||||05-DEC-06
17551|Surprise Creek Formation|49041|5|Briefly described|Table 1|||||||||
17551|Surprise Creek Formation|50100|5|Briefly described|p11, p13 Fig. 4, p19|Statherian|Statherian|Disconformably, unconformably and nonconformably overlies Leichhardt Volcanics and Kalkadoon Granodiorite.  Geological Province: Kalkadoon-Ewen Province / Western Fold Belt Province.||||||
17551|Surprise Creek Formation|50332|4|Described|p16, p20|Paleoproterozoic|Paleoproterozoic|Disconformably, unconformably and nonconformably overlies the Bigie Formation, Leichhardt Volcanics + Kalkadoon Granodiorite. Age: ~1700-1640Ma.Geol Prov: Western Fold Belt Province. Sedimentary rocks and subordinate bimodal volcanics.||||||07-FEB-11
17551|Surprise Creek Formation|50550|5|Briefly described|p1139 Fig.2, p1141 Fig.4||Statherian|Overlies Fiery Creek Volcanics at a syn-rift unconformity. Conformably overlain by Torpedo Creek Quartzite. Geological Province: Western Fold Belt.||||||19-DEC-07
17551|Surprise Creek Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arenite; minor conglomerate, shale, siltstone.||||||
17551|Surprise Creek Formation|60558|5|Briefly described|p4 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt.||||||03-JUN-09
17551|Surprise Creek Formation|61204|5|Briefly described|p538|||Geological Province: Mount Isa Inlier. Underlain by Eastern Creek Volcanics; unconformably overlies Haslingden Group. Siltstones; sandstones; conglomerates.||||||31-MAY-07
17551|Surprise Creek Formation|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
17551|Surprise Creek Formation|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Ages: 1688+/-6Ma, 1687+/-5Ma and 1688+/-5Ma (SHRIMP, Jackson et al 2005) from tuffs or shallow level, peperitic units.||||||
17551|Surprise Creek Formation|61929|5|Briefly described|p128 Fig. 2|||||||||
17551|Surprise Creek Formation|61936|5|Briefly described|p194 Fig. 6|||Dominantly siliciclastic succession.||||||
17551|Surprise Creek Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Surprise Ck Fm.|1694+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
17551|Surprise Creek Formation|62535|5|Briefly described|p672-673|Statherian|Statherian|Several other (similar) ages are given.|1688 +/- 6 Ma.|||Unconformably overlies Bigie Formation.||
17551|Surprise Creek Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Basal pebble to boulder conglomerate with clasts of quartz, quartzite and rhyolite in matrix of pink medium to coarse grained sublithic sandstone.||||||06-MAY-13
17551|Surprise Creek Formation|63023|5|Briefly described|p1024 Fig. 1, p1025 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: ~1709+/-3Ma. Geological Province: Calvert Superbasin.||||||07-NOV-08
17551|Surprise Creek Formation|63109|6|Mentioned|p1112, p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone.||||||01-SEP-08
17551|Surprise Creek Formation|63111|5|Briefly described|p1162, p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Overlain by Torpedo Creek Quartzite, underlain by Fiery Creek Volcanics. Age: 1690+/-7Ma. Geological Province: Calvert Superbasin. Consists of sandstone with conglomerate at the base of formation.||||||07-FEB-11
17551|Surprise Creek Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Calvert Superbasin. Part of Prize supersequence.|1709 Ma.|Of the Myally Subgroup||Overlies Fiery Creek Formation.||
17551|Surprise Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Calvert superbasin.||Of the Prize supersequence.||Overlies Fiery Creek Volcanics.||
17551|Surprise Creek Formation|63115|6|Mentioned|1279 Fig.4, p1281, |||Calvert superbasin.||||||
17551|Surprise Creek Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Calvert superbasin. Material properties detailed.||||||
17551|Surprise Creek Formation|63866|5|Briefly described|p58|||||||Overlies the Bigie Formation.||
17551|Surprise Creek Formation|64250|5|Briefly described|p25 fig 10, p11 fig 3, p27, p18|||Western Fold Belt, Mount Isa Inlier. Deeper water facies carbonaceous siltstone. Cu mineralisation.|1700-1690|||Is overlain by Torpedo Creek Quartzite and Warrina Park Quartzite. Correlated with Mount Albert Group in Eastern Fold Belt.|Deeper water facies carbonaceous siltstone.|
17551|Surprise Creek Formation|64367|5|Briefly described|p555  Fig. 1c|Paleoproterozoic|Paleoproterozoic|Age: 1688+/-5Ma.||||||07-FEB-11
17551|Surprise Creek Formation|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
17551|Surprise Creek Formation|64726|6|Mentioned|p83 Fig.2.|||||||||
17551|Surprise Creek Formation|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Mount Isa Basin.||||||
17551|Surprise Creek Formation|64834|5|Briefly described|p12, p13 Fig.2, p31-32|||Calvert Superbasin. Western Succession of Mount Isa Basin.||||Unconformably overlies Eastern Creek Volcanics.|Sandstone, with pebble conglomerate near base.|
17551|Surprise Creek Formation|65228|5|Briefly described|p21, p23, Figs.04, 09, 10.|||Leichhardt River Fault Trough. Studied in detail by Domagala et al. (2000).||||Unconformably overlies Bigie Formation, Myally Subgroup and Eastern Creek Volcanics.||
17551|Surprise Creek Formation|65337|4|Described|p v, pp19-20.|Calymmian|Statherian|Calvert Superbasin. Thin siliciclastic veneer, from zero to 2000 m thick, of braided fluvial deposits, with local alluvial fan deposits at base.|1700-1690 Ma.|||Unconformably overlies Carrara Range Group. Is unconformably overlain by Gunpowder Creek or Drummond Formations of the McNamara Group.|Basal conglomerates, poorly-sorted and matrix-supported, sub-rounded to well-rounded pebbles and cobbles of quartz, quartzite and quartz sandstone, some rhyolite clasts; under white to pink, medium- to coarse-grained, sublithic to quartz sandstone.|
17551|Surprise Creek Formation|65396|5|Briefly described|p16, p82, p175, p184, p190, p201, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform, Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt.|1700 - 1690 Ma|||Overlain by Torpedo Creek Quartzite, Warrina Park Quartzite.|Sandstone, calcareous shales, pelites and mafic volcanics.|04-APR-17
17551|Surprise Creek Formation|66529|6|Mentioned|p34|||Calvert Superbasin. Hosts some uranium prospects.||||||
17551|Surprise Creek Formation|66824|6|Mentioned|p148|||||||Unconformably overlies Fiery Creek Volcanics. Is overlain unconformably by Mount Isa Group.||
17551|Surprise Creek Formation|67026|6|Mentioned|p336 Fig.3.|Statherian|Statherian||1694 +/- 3 Ma (Page et al. 2000).|||||24-APR-12
17551|Surprise Creek Formation|67323|5|Briefly described|p8, p11, p25, p34, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Calvert Superbasin. Widespread unit in the Mount Isa Inlier. Ages by Page et al. (2000); Jackson et al. (2005) respectively.|1694 +/-3 Ma; 1687.7 +/-4.6 Ma.|||Unconformably overlies Quilalar Formation, Fiery Creek Volcanics, Myally Subgroup, Eastern Creek Volcanics (locally).|Quartzite, sandstone, calcareous sandstone, conglomerate, siltstone, shale|
17551|Surprise Creek Formation|67499|6|Mentioned|p948|||||Of Mount Isa Group?||||
17551|Surprise Creek Formation|68021|5|Briefly described|p135 fig 4|Statherian|Statherian|Prize Supersequence,  Calvert Superbasin, Western Succession. Environment changing from near-shore to deltaic or shallow marine.||||Overlies Fiery Creek Volcanics unconformably, overlain by McNamara Group, Mount Isa Group unconformably. Intruded by Sybella Granite? Part Equivalent to Roxmere Quartzite.|?Several cycles of upward-fining mainly siliciclastic sedimentation and increasing amounts of thinly laminated carbonaceous shale or rhythmite towards top.|
17551|Surprise Creek Formation|68146|5|Briefly described|p3, p189, p199, p203|||Age of tuff beds within the unit.|c.1688 Ma; Jackson et al. (2005).|||Overlies Fiery Creek Volcanics. Is overlain by Bularnu Formation.||
17551|Surprise Creek Formation|68542|5|Briefly described|p7|||Surprise Creek beds.|||||Sandstone, quartzite and conglomerate.|
17551|Surprise Creek Formation|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
17551|Surprise Creek Formation|68575|5|Briefly described|p3, p37, p127|||SHRIMP age of "shallow-level peperitic intrusives". Also has detrital zircon maximum deposition ages of 1745 +/- 6 Ma and 1731 +/- 12 Ma (Neumann et al., 2009).|1688 +/- 5 Ma (Jackson et al., 2005).|||||
17551|Surprise Creek Formation|68576|5|Briefly described|Q_2: p7||||||||Sandstone, quartzite, conglomerate.|
17551|Surprise Creek Formation|68732|5|Briefly described|p160-162, p165 Fig.3, p168 Fig.5|||Undulatory rhythmite facies common. Of the Prize Supersequence. Sedimentary depositional ages.|1688 +/- 5, 1688 +/- 6 Ma||||Mainly very fine-grained arkosic sandstones. Includes cross-stratified quartzites and pebbly quartzites at the base, and fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|01-DEC-17
17551|Surprise Creek Formation|69056|5|Briefly described|p54|||Mount Isa Western Succession; Calvert Superbasin.|||||Sandstone.|
17551|Surprise Creek Formation|69222|5|Briefly described|p221, p222 Fig.2|Statherian|Statherian|Western Fold Belt. Associated with the Mount Isa Rift Event.||||Overlies Carters Bore Rhyolite, overlain by Mount Isa Group, McNamara Group||09-FEB-18
17551|Surprise Creek Formation|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Overlies Bigie Formation. Is intruded by Weberra Granite. Is overlain by Mount Isa Group.||25-JAN-19
17551|Surprise Creek Formation|69433|4|Described|p18:2-3, 5-9|Statherian|Statherian|Rawlings et al. (2008); previously mapped (Sweet, 1984) as part of now-obsolete Musselbrook Formation. Southern succession, Lawn Hill Platform. Widespread in the Mount Isa region. Up to 450m thick. Braided fluvial, with local alluvial fan at base, deposits.||||Unconformably overlies Carrara Range Group. Is overlain by Mount Isa and McNamara Groups conformably or disconformably.|Basal lenses and beds of sub- to well-rounded pebble to boulder conglomerate with a coarse lithic sandstone matrix, intertonguing with and overlain by white to pink, thickly to very thickly bedded, medium to coarse sublithic to quartz sandstone.|12-JUL-16
17551|Surprise Creek Formation|69591|5|Briefly described|p29, p37-40, p44, p56, p107|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Part of the Prize Supersequence. Locally there was a hiatus between the lower and upper parts of this unit. Fluvial-shallow-marine deposits. Shows abrupt thickness changes across normal faults, forming wedge-shaped stratal geometries.|1688 +/- 5 Ma (Jackson et al., 2005)..|||Is overlain by Moondarra Siltstone.|Basal quartzite grading upwards into siltstone and minor shale. Also described on p56 as quartzite, sandstone, calcareous sandstone, conglomerate, siltstone, shale.|
17551|Surprise Creek Formation|69673|5|Briefly described|p53|||Up to 450m thick.|||||Conglomerate and sandstone.|
17551|Surprise Creek Formation|70282|5|Briefly described|p544 Tb.1|||Cover sequence 4, Mount Isa. Alluvial fan or shallow-marine deposits.|> 1652 Ma|||Overlain by Mount Isa Group|Conglomerate, sandstone and siltstone,|13-FEB-18
17551|Surprise Creek Formation|70283|6|Mentioned|p25|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group||Overlies Haslingden Group.||14-FEB-18
17551|Surprise Creek Formation|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Five facies associations are separately mapped.|||||Siltstone, sandstone, quartzite, shale, conglomerate, ferruginous oolite marker beds.|
17551|Surprise Creek Formation|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Five facies associations are separately mapped.|||||Siltstone, sandstone, quartzite, shale, conglomerate, ferruginous oolite marker beds.|
17551|Surprise Creek Formation|70864|5|Briefly described|p79, p74 Fig 2, p82|||||?McNamara Group?|Overlies Gunpowder Creek Formation|||14-FEB-18
17551|Surprise Creek Formation|71592|5|Briefly described|Appendix A.|||Kalkadoon-Leichhardt Domain, Mount Isa Orogen.|1691+/-6.9 Ma (MDA: U-Pb zircon SHRIMP)||||Chert, sandstone.|
17551|Surprise Creek Formation|71606|5|Briefly described|p137|Statherian|Statherian|Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Mount Isa Group.||
17551|Surprise Creek Formation|71960|5|Briefly described|p85, p83, p87, 104, 105, 106|Proterozoic|Proterozoic|In Paroo Range overlies an unconformity. Herein added to lower Mount Isa Group. Wedges out to west and south.||Of Mount Isa Group.||Unconformably to conformably overlain by Warrina Park Quartzite. Unconformably overlies/truncates Haslingden Group rocks.||
17551|Surprise Creek Formation|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Western Fault Zone. From base: heterolithic inshore to transitional marine; fan, distributive to coastal; channel fill.||Of Mount Isa Group|||Ferruginous sandstone, dolostone, stromatolite, chert; shale, siltstone, sandstone; feldspathic sandstone; channel-fill framework conglomerate.|
17551|Surprise Creek Formation|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Age given as U-Pb zircon sedimentary depositional age. Shown as located in the Lawn Hill Platform, Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province and the eastern part of the South Nicholson Basin.|1688 +/-5 Ma|||Shown as unconformably overlying Fiery Creek Volcanics and Bigie Formation and underlies Torpedo Creek Quartzite and Warrina Park Quartzite.||
17551|Surprise Creek Formation|72527|4|Described|p1, 3, 5, 7, 9, 91, p147-160, p193, 194|Statherian|Statherian|South Nicholson Basin. Previously included in the obsolete Musselbrook Formation. Two samples dated from Mt Druumond area, NT: both quartz sandstone, 1858+/-5 Ma, 1743+/-26 Ma, Pb/Pb SHRIMP. Previous studies in Qld established depositional age ~1690-1680 Ma. Uncertain or unassigned stratigraphic affinity. Up to 200 m thick. Type location in the Lawn Hill region, Qld c. 300km southeast of Mount Drummond. Depositional environment is probably a proximal braided fluvial system, with local alluvial fans.|1743+/-26 Ma, 1858 +/- 5 Ma max depositional ages|||Unconformably overlies Top Rocky Rhyolite and unconformably underlies McNamara Group (Drummond Formation).|Well-rounded pebble to boulder conglomerate (with rhyolite clasts near the base), interlayered with sub-lithic to quartz sandstone (displaying small scale trough beds and current lineations).|
17551|Surprise Creek Formation|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain and Kalkadoon-Leichhardt Domain. Shown as older than the Isan Orogeny (1590-1500 Ma).||||Shown as partially equivalent in age and older than Garden Creek Porphyry.|Convoluted fine sandstone and siltstone; ferruginous gossanous sandstone. Buff, pink, white, and pale bluish grey thin-bedded fine to medium labile and ferruginous feldspathic sandstone, conglomerate, mud flake-shale pellet beds and quartzite.|
17551|Surprise Creek Formation|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichardt River Domain and Kalkadoon-Leichhardt Domain. Shown as older than the Isan Orogeny (1590-1500 Ma).||||Shown as partially equivalent in age and older than Garden Creek Porphyry.|Convoluted fine sandstone and siltstone; ferruginous gossanous sandstone. Buff, pink, white, and pale bluish grey thin-bedded fine to medium labile and ferruginous feldspathic sandstone, conglomerate, mud flake-shale pellet beds and quartzite.|
17551|Surprise Creek Formation|72889|6|Mentioned|p6 Fig.i.|||||||||
17551|Surprise Creek Formation|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Located in the Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt and the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional age (Ma).|1688 +/- 5 Ma|Of Prize supersequence.||Shown as unconformably overlying Fiery Creek Volcanics and Bigie Formation and underlies Torpedo Creek and Warrina Park Quartzite.||
17551|Surprise Creek Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||||Unconformably underlain by Top Rocky Rhyolite (Carrara Range Group). Unconformably overlain by Drummond Formation (McNamara Group).||
17551|Surprise Creek Formation|73042|6|Mentioned|p4|Statherian|Statherian|The Surprise Creek Formation is recorded at two different chronostratigraphic levels in the South Nicholson Basin region / Mount Isa Province, but there is no explanation. The unit is written as Surprise Creek Formation* in the older instance, in Carrara Range Group. South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age) from the chronostratigraphically higher of the two instances of the unit, further east,  in Fig.1.2. overlain by Torpedo Creek/Warrina Park Quartzite.|1688 +/- 5 Ma (see comments and Fig.1.2)|Nil and Carrara Range Group (see comments)||Drummond Formation overlies unconformably. Top Rocky Rhyolite, Fiery Creek Volcanics/Bigie Formation underlie unconformably.||
17551|Surprise Creek Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
17551|Surprise Creek Formation|73083|6|Mentioned|p72|||||||||
17551|Surprise Creek Formation|73137|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|||||||
17551|Surprise Creek Formation|73144|6|Mentioned|p9-10|||Calvert Superbasin. Prize Supersequence. Deposited in a coastal plain, nearshore environment with some below storm wavebase deposits (Southgate et al., 2000).|||||Sandstone, conglomerate and siltstone.|
17551|Surprise Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) and Leichhardt River Domains.|1694+/-3 Ma, 1687+/-4 Ma, 1682+/-19 Ma||||Clastics, siliciclastics.|
17565|Suttor Formation|22675|5|Briefly described|p89|Cenozoic|Cenozoic|||||||19-NOV-08
17565|Suttor Formation|22995|5|Briefly described|p361|Tertiary|Tertiary|||||||
17565|Suttor Formation|23052|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
17565|Suttor Formation|23078|5|Briefly described|p708|Tertiary|Tertiary|||||||
17565|Suttor Formation|23080|5|Briefly described|p696||Tertiary|||||||
17565|Suttor Formation|23081|5|Briefly described|p692||Tertiary|||||||
17565|Suttor Formation|23161|4|Described|p5,7,34 fig4 table1|Tertiary|Tertiary|||||||
17565|Suttor Formation|23422|5|Briefly described|p186|Miocene|Miocene|||||||
17565|Suttor Formation|23430|4|Described|p504 Table 14.5|||Also see p527. Kalpowar Basin Province.||||||
17565|Suttor Formation|23986|4|Described|p92|||Geological Province: Drummond Basin.||||||
17565|Suttor Formation|23988|4|Described|p10|Tertiary|Tertiary|See also page 52 Fig. 35.||||||
17565|Suttor Formation|24031|5|Briefly described|p2, p3 Fig. 1, p4 Fig. 2, p5, p13|Palaeocene|Palaeocene|Underlain unconformably by Silver Hills Formation. Thickness: 10m. Sandstones. Equivalent to Southern Cross Formation. See also p15 Tb. 4, p16, p24, p27, p30.||||||
17565|Suttor Formation|32493|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
17565|Suttor Formation|32553|4|Described|p38|||||||||
17565|Suttor Formation|32556|4|Described|Table 4|||Tertiary||||||
17565|Suttor Formation|33353|6|Mentioned|p457|||||||||
17565|Suttor Formation|34314|5|Briefly described|Table 3|||See p10. Tertiary.||||||18-SEP-18
17565|Suttor Formation|34389|4|Described|Table 2|||Tertiary.||||||18-SEP-18
17565|Suttor Formation|35872|6|Mentioned|p454|||||||||
17565|Suttor Formation|36472|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
17565|Suttor Formation|37073|6|Mentioned|p99|||||||||
17565|Suttor Formation|37078|6|Mentioned|Fig.1|||||||||
17565|Suttor Formation|37458|6|Mentioned|Table 1|||||||||
17565|Suttor Formation|37607|5|Briefly described|p336|||See also Figs.7 and 8.||||||
17565|Suttor Formation|39445|5|Briefly described|Table 14|||Eocene. Gold. See also p150 & p152.||||||18-SEP-18
17565|Suttor Formation|39708|6|Mentioned|p481|||||||||
17565|Suttor Formation|39942|6|Mentioned|p469|||||||||
17565|Suttor Formation|40968|6|Mentioned|p277|||||||||
17565|Suttor Formation|41650|6|Mentioned|Fig.2|||||||||
17565|Suttor Formation|42281|5|Briefly described|p81|Tertiary||||||||
17565|Suttor Formation|42474|6|Mentioned|p29|||Mount Coolon 1:250 000 sheet.||||||
17565|Suttor Formation|42701|3|Fully described|p75|||||||||
17565|Suttor Formation|42899|5|Briefly described|p347|||||||||
17565|Suttor Formation|42932|6|Mentioned|Fig.13|||||||||
17565|Suttor Formation|43051|4|Described|p132|||||||||
17565|Suttor Formation|43099|5|Briefly described|p7|||||||||
17565|Suttor Formation|43204|5|Briefly described|Map Legend||Tertiary|||||||23-DEC-11
17565|Suttor Formation|43213|5|Briefly described|p10, p160, p239|Miocene|Oligocene|Early to Mid-Tertiary. Mount Coolon area. Generally deeply weathered, commonly with a ferruginous duricrust capping. Basalt interbeds dated at 23-29 Ma (Hutton et al., 1991).|||||Fluvial sequence of clays, silt and sand, locally interbedded with basalts.|
17565|Suttor Formation|43391|5|Briefly described|Map legend|Tertiary|Tertiary|Mainly quartz sandstone.||||||23-JUN-04
17565|Suttor Formation|43706|5|Briefly described|p5||Tertiary|||||||
17565|Suttor Formation|43727|5|Briefly described|p7||Tertiary|||||||
17565|Suttor Formation|43988|14|Not recorded|Map Legend||Tertiary|||||||
17565|Suttor Formation|43998|14|Not recorded|Map||Tertiary|||||||
17565|Suttor Formation|44000|2|Defined|Tb.1,2,p.6,7,43-4,47|||p59.||||||18-SEP-18
17565|Suttor Formation|44001|14|Not recorded|Map Legend|||||||||
17565|Suttor Formation|44009|14|Not recorded|p68,78|||||||||
17565|Suttor Formation|44245|5|Briefly described|Map Legend||Tertiary|||||||
17565|Suttor Formation|44331|14|Not recorded|Map Legend||Tertiary|||||||
17565|Suttor Formation|45073|6|Mentioned|Fig.|||Geol. map Drummond Basin.||||||18-SEP-18
17565|Suttor Formation|45151|5|Briefly described|p35|||||||||
17565|Suttor Formation|46902|6|Mentioned|Table 1|||Correlation chart for Cainozoic land-surfaces||||||
17565|Suttor Formation|48841|2|Defined|p15,36-40,48,Tb.I||Tertiary|Overlies Anakie Metamorphics, Bulgonunna Volcanics. Permian sediments.||||||
17565|Suttor Formation|48843|2|Defined|p.37,47,49||Tertiary|Freshwater deposits; ?Tertiary.||||||
17565|Suttor Formation|48915|6|Mentioned|Table 1|||Tertiary.||||||18-SEP-18
17565|Suttor Formation|48922|4|Described|p48|||||||||
17565|Suttor Formation|50153|5|Briefly described|p4, p9, p18|Paleocene|Cenozoic|Correlated with the Southern Cross Formation to the north. Overlain by a 53 Ma basalt at Mount Dalrymple, so possibly Paleocene in age. Older than Campaspe Formation. May have widespread subsurface distribution.|||||Dominantly fluviatile and lacustrine sandstones and siltstones.|15-MAR-13
17565|Suttor Formation|60659|5|Briefly described|p22, p44-45|Middle Tertiary|Middle Tertiary|Includes fluvial sandstone, sandy muds and channel sands overlain by lacustrine oil shale, claystone, mudstone, sandstone, sands, diatomite and colluvial deposits. Geological Province: Drummond Basin.||||||07-FEB-11
17565|Suttor Formation|61814|5|Briefly described|p20|Tertiary|Tertiary|Thick sequence of unlithified sediments with lignite lenses interpreted to be equivalent to Southern Cross Formation in the Charters Towers area. Intensely weathered. Geological Province: Drummond Basin.||||||08-FEB-10
17565|Suttor Formation|66084|5|Briefly described|Map legend|Tertiary|Tertiary|Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.||||||
17565|Suttor Formation|66086|5|Briefly described|Map legend|Tertiary|Tertiary|Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.||||||
17565|Suttor Formation|68404|5|Briefly described|Map legend|Neogene|Paleogene|Shown as Tertiary age.|||||Quartz sandstone, clayey sandstone, mudstone and conglomerate: fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross and Springvale Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya, Takura and Water Park Creek beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
17565|Suttor Formation|68679|5|Briefly described|p364|Paleogene|Paleogene|||||||
17565|Suttor Formation|68901|6|Mentioned|p2 Fig. i|Paleogene|Paleogene|||||||27-SEP-18
17565|Suttor Formation|69599|5|Briefly described|p584-585, p592-593|Miocene|Paleocene|Malone et al. (1964). Charters Towers and northern Drummond Basin. A complex mosaic of paleovalley fill and lacustrine sediments deposited in a diffuse basin with interconnected depocentres. Generally <60m thick; may reach 150m. Age is unresolved (discussion). Silcrete and ferricrete development (Featherby Surface) occurred in late Eocene-Oligocene.||||Correlated with Biloela beds; Southern Cross, Exevale, Emerald and Duarings Formations.|General succession is a basal fluvial sandstone overlain by lacustrine mudstone with common oil shale, sandy stringers and rare diatomite, in turn overlain by coarser fluvial sandstone and rare conglomerate. In the E, interbedded with basalt flows.|
17565|Suttor Formation|69952|6|Mentioned|p85|Paleogene|Paleogene|||||||
17565|Suttor Formation|70740|5|Briefly described|p7, p73, p102, p106, p130|Tertiary|Tertiary|Drummond Basin.||||Unconformably overlies the Bimurra Volcanics. Overlies the Wirralie Granodiorite, Locharwood Rhyolite.|Flat-lying sandstones.|
17565|Suttor Formation|72297|5|Briefly described|p724, p726|Cenozoic|Cenozoic|Kaolin deposits at Bungobine and Yacamunda, W of Mount Coolon; also diatomite.|||||A cyclical lacustrine sequence of kaolin alternating with oil shales.|
17565|Suttor Formation|73035|5|Briefly described|Map legend|Neogene|Paleogene||||||Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|73036|5|Briefly described|Map legend|Eocene|Paleocene||||||Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|73037|5|Briefly described|Map legend|Eocene|Paleocene||||||Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|73038|5|Briefly described|Map legend|Eocene|Paleocene||||||Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|73040|5|Briefly described|Map legend|Eocene|Paleocene||||||Quartz sandstone, clayey sandstone, mudstone and conglomerate; fluvial and lacustrine sediments; minor interbedded basalt.|
17565|Suttor Formation|75060|5|Briefly described|p40-44, 55, 57|Miocene|Oligocene|Malone et al. (1964). Northwest Bowen Basin. Deposition in paleochannels (fluvial and lacustrine). Extensively exposed in the Suttor River catchment area. 60-150m thick.|||||Variably composed of basal sandstone; lacustrine mudstone, clayey materials, lignite and oil shale; then coarse sandstone. These sediments either interbedded with or overlain by weathered basalt flows up to 80m thick|
17576|Swanfels Trachyte Member|39969|6|Mentioned|p9|||See also P10||||||
17576|Swanfels Trachyte Member|48917|6|Mentioned|p7|||Refers Stevens (1965)||||||
17576|Swanfels Trachyte Member|73450|6|Mentioned|p92|||Of Stevens, 1965; Grenfell, 1984; Ewart & Grenfell, 1985. Never described in detail.||Governors Chair Volcanics|||Felsic.|29-SEP-22
17583|Swift Formation|13995|5|Briefly described|p75|Middle Ordovician|Early Ordovician|Georgina Basin. Rostroconch species listed.||||||
17583|Swift Formation|22954|5|Briefly described|Fig1p6,Fig5p16,23-4|Tertiary|Warendan|Correlates with Digby Peaks Breccia.||||||
17583|Swift Formation|24065|4|Described|p235|Early Ordovician|Late Cambrian|Geological Province: Georgina Basin.  Maximum thickness: 20m.||||||
17583|Swift Formation|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|31572|4|Described|Fig. 1|||L.Ord.||||||
17583|Swift Formation|32576|6|Mentioned|p50|||Potential aquifer||||||
17583|Swift Formation|33111|4|Described|p43|||||||||
17583|Swift Formation|33738|6|Mentioned|p49|||||||||
17583|Swift Formation|35121|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
17583|Swift Formation|35139|4|Described|Table.2|||||||||
17583|Swift Formation|35936|6|Mentioned|p614|||||||||
17583|Swift Formation|36645|6|Mentioned|p312|||||||||
17583|Swift Formation|37413|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|37572|4|Described|p162|||See also Fig.8||||||
17583|Swift Formation|38444|5|Briefly described|p118|||||||||
17583|Swift Formation|38532|4|Described|Fig.1|||||||||
17583|Swift Formation|38608|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17583|Swift Formation|39445|5|Briefly described|Table 4|||See also p64.||||||05-DEC-06
17583|Swift Formation|39690|6|Mentioned|Fig.2|||||||||
17583|Swift Formation|40127|6|Mentioned|p8|||||||||
17583|Swift Formation|40136|5|Briefly described|p40|||||||||
17583|Swift Formation|42354|5|Briefly described|p11|||||||||
17583|Swift Formation|43807|6|Mentioned|Fig.3,p348|||||||||
17583|Swift Formation|44358|6|Mentioned|p19|||Boulia area.||||||
17583|Swift Formation|44361|14|Not recorded|Map Legend||Early Ordovician|||||||
17583|Swift Formation|44362|4|Described|p11,Tb.1||Early Ordovician|||||||
17583|Swift Formation|44469|14|Not recorded|p.19|||Similar to Kelly Creek Formation lithology.||||||05-DEC-06
17583|Swift Formation|44543|2|Defined|p33||Early Ordovician|Overlies Ninmaroo Formation.||||||
17583|Swift Formation|44920|14|Not recorded|Map Legend, Sheet 4||Early Ordovician|||||||
17583|Swift Formation|45051|6|Mentioned|p4|||See also p10.23,Fig.3. Lower Ordovician age.||||||05-DEC-06
17583|Swift Formation|45052|2|Defined|p126|Early Ordovician|Early Ordovician|See also p37.||||||05-DEC-06
17583|Swift Formation|45058|6|Mentioned|Fig. 11|||Correlation||||||
17583|Swift Formation|45079|6|Mentioned|p12|||Map legend on p12.||||||05-DEC-06
17583|Swift Formation|45115|6|Mentioned|p6|||||||||
17583|Swift Formation|45166|5|Briefly described|Table 15|||||||||
17583|Swift Formation|46897|6|Mentioned|Fig.2|||||||||
17583|Swift Formation|46958|6|Mentioned|p195|||See also Fig.2.||||||
17583|Swift Formation|50100|5|Briefly described|p22|Early Ordovician|Early Ordovician|Comprises chert with siltstone, sandstone, silicified coquinite, limestone and dolomite interbeds; highly fossiliferous.  Overlies the Ninmaroo Formation.||||||
17583|Swift Formation|60359|5|Briefly described|Map Legend|Ordovician|Ordovician|Siltstone, sandstone, chert.||||||
17583|Swift Formation|63450|5|Briefly described|p78 Fig. 5, p82|Arenig|Tremadoc|Overlies Ninmaroo Formation as a regolith derived from karstification of the Ninmaroo Formation. Geological province: Georgina Basin, Burke River Structural Belt.||||||07-FEB-11
17583|Swift Formation|64068|3|Fully described|p75, 74, 75|Early Ordovician|Early Ordovician|Diverse fauna. 20 m thick. Regolith preferentially developed over weathered surfaces of Corrie and Datson Members of Ninmaroo Formation. Correlated with Kelly Creek Formation.||Of Cockroach Group.|||Chert, siltstone, sandstone, silicified coquinite, limestone, dolostone.|04-APR-12
17583|Swift Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin.||Cockroach Group.||Overlies Ninmaroo Formation.|Siltstone, sandstone, coquinite (all silicified in part) chert|
17583|Swift Formation|67870|6|Mentioned|p43|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin.||||||
17583|Swift Formation|69443|5|Briefly described|p28:7, 25-26|Early Ordovician|Early Ordovician|Southern Georgina Basin. Regarded as a subaerial regolith discordant on the uppermost Ninmaroo Formation.||Cockroach Group.||Conformably overlies Ninmaroo Formation.||12-JUL-16
17583|Swift Formation|69591|5|Briefly described|p87, p93-94|Ordovician|Ordovician|Burke River Structural Belt, Georgina Basin. About 20m thick. Contains trilobites, brachiopods and a Bendigonian-age graptolite. Has undergone considerable diagenesis; interpreted as the silicification product of the upper two members (encrinite and dolomite) of the Ninmaroo Formation.||||Is laterally equivalent to the upper part of Ninmaroo Formation; locally overlies it unconformably. Unconformably overlies Beetle Creek Formation.|Bedded chert with interbeds of siltstone, sandstone, silicified coquinite and limestone.|
17583|Swift Formation|69673|6|Mentioned|p114 fig 92|||||Cockroach Group||Overlain by Kelly Creek Formation, overlies Chabalowe Formation, Arrinthrunga Formation||
17589|Sybella Granite|22498|6|Mentioned|Fig1 P234||Statherian|||||||
17589|Sybella Granite|22644|6|Mentioned|19|||Geol province Mount Isa Basin||||||
17589|Sybella Granite|22692|6|Mentioned|p765|||||||||
17589|Sybella Granite|23363|5|Briefly described|344 Fig.3|||||||||
17589|Sybella Granite|23396|5|Briefly described|p419|Statherian|Statherian|Age: 1671+/-8Ma.||||||05-DEC-06
17589|Sybella Granite|23398|5|Briefly described|p449|Statherian|Statherian|Age: ~1670Ma.||||||05-DEC-06
17589|Sybella Granite|23408|5|Briefly described|p510 Fig.1, p513 Fig. 2, p527|||||||||15-JUN-09
17589|Sybella Granite|23458|6|Mentioned|p114, p127|||In the Eastern Fold Belt.||||||27-AUG-07
17589|Sybella Granite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1670+/-8 Ma||||||02-NOV-07
17589|Sybella Granite|23969|6|Mentioned|p1371 Fig.2|||Geological Province: Mount Isa Inlier.||||||
17589|Sybella Granite|23972|5|Briefly described|p1422|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Isa Inlier.  Age: ~1660Ma.||||||
17589|Sybella Granite|24033|6|Mentioned|p15|||||||||
17589|Sybella Granite|24197|5|Briefly described|p130|Paleoproterozoic|Paleoproterozoic|Of Sybella Suite. Geological province: Mount Isa Inlier.||||||07-FEB-11
17589|Sybella Granite|24253|5|Briefly described|p9|Proterozoic|Proterozoic|Age: 1660 Ma. Geological Province: Mount Isa Block.||||||
17589|Sybella Granite|24254|5|Briefly described|p17, p24|Proterozoic|Proterozoic|Geological Province: Mount Isa Block. Age: ca. 1660-1670 Ma.||||||
17589|Sybella Granite|24419|5|Briefly described|p17, p12 Fig.4, p15 Fig.6|Proterozoic|Proterozoic|Of the Sybella Suite.||||||
17589|Sybella Granite|24432|5|Briefly described|p564 Fig.4|Statherian|Statherian|Geological Province: Mount Isa Inlier.||||||
17589|Sybella Granite|30531|6|Mentioned|p22|||||||||
17589|Sybella Granite|30534|6|Mentioned|p300|||See also p302,305.||||||05-DEC-06
17589|Sybella Granite|30535|6|Mentioned|p404|||Refers age Warrina Park Quartzite||||||
17589|Sybella Granite|30536|6|Mentioned|p100|||||||||
17589|Sybella Granite|30721|5|Briefly described|p53|||See also p54.||||||05-DEC-06
17589|Sybella Granite|30723|4|Described|p340|||Rb/Sr 1655m.y. Isotopic plot p346. See also p348.||||||05-DEC-06
17589|Sybella Granite|30724|6|Mentioned|p74|||Age given||||||
17589|Sybella Granite|30725|4|Described|p576|||||||||
17589|Sybella Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|32041|4|Described|p353|||||||||
17589|Sybella Granite|32042|5|Briefly described|p36|||||||||
17589|Sybella Granite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|32660|5|Briefly described|Table 5|||||||||
17589|Sybella Granite|32818|5|Briefly described|p17|||Age||||||
17589|Sybella Granite|32951|6|Mentioned|p1276|||Consists of several phases||||||
17589|Sybella Granite|32952|6|Mentioned|p1188|||Precambrian||||||
17589|Sybella Granite|32959|6|Mentioned|p31|||||||||
17589|Sybella Granite|33482|6|Mentioned|p6|||||||||
17589|Sybella Granite|33893|4|Described|p35|||||||||
17589|Sybella Granite|33896|5|Briefly described|p465|||Foliations discussed||||||
17589|Sybella Granite|33897|6|Mentioned|p1280|||||||||
17589|Sybella Granite|33898|6|Mentioned|p232|||||||||
17589|Sybella Granite|33900|5|Briefly described|p21|||||||||
17589|Sybella Granite|34955|6|Mentioned|p227|||Age dating.||||||
17589|Sybella Granite|35074|6|Mentioned|Fig.2|||||||||
17589|Sybella Granite|35114|6|Mentioned|p203|||||||||
17589|Sybella Granite|35121|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|35139|4|Described|Table.2|||See also p10.||||||05-DEC-06
17589|Sybella Granite|35146|6|Mentioned|p469|||||||||
17589|Sybella Granite|35167|6|Mentioned|p151|||||||||
17589|Sybella Granite|35286|6|Mentioned|p156|||||||||
17589|Sybella Granite|35950|6|Mentioned|p305|||||||||
17589|Sybella Granite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|36548|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|37217|6|Mentioned|p650|||||||||
17589|Sybella Granite|37371|6|Mentioned|p368|||||||||
17589|Sybella Granite|37459|6|Mentioned|p423|||||||||
17589|Sybella Granite|37462|4|Described|Table4.VII|||||||||
17589|Sybella Granite|37565|6|Mentioned|Fig.5|||||||||
17589|Sybella Granite|37568|6|Mentioned|p85|||||||||
17589|Sybella Granite|37572|6|Mentioned|Fig.8|||||||||
17589|Sybella Granite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17589|Sybella Granite|37862|6|Mentioned|p586|||||||||
17589|Sybella Granite|38232|6|Mentioned|p83|||See also p89.||||||05-DEC-06
17589|Sybella Granite|38276|6|Mentioned|Fig.1|||||||||
17589|Sybella Granite|38350|4|Described|p20|||See also p10.||||||05-DEC-06
17589|Sybella Granite|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||25-AUG-04
17589|Sybella Granite|38560|6|Mentioned|p115|||||||||
17589|Sybella Granite|38598|6|Mentioned|p208|||||||||
17589|Sybella Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17589|Sybella Granite|38919|6|Mentioned|p496|||||||||
17589|Sybella Granite|39362|6|Mentioned|p1468|||||||||
17589|Sybella Granite|39445|5|Briefly described|p41|||See also p36 and Table 2.||||||05-DEC-06
17589|Sybella Granite|39622|6|Mentioned|p24|||See also Appendix||||||
17589|Sybella Granite|39690|6|Mentioned|p98|||||||||
17589|Sybella Granite|39822|6|Mentioned|p220|||||||||
17589|Sybella Granite|39934|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|40623|5|Briefly described|p102|||||||||
17589|Sybella Granite|40840|6|Mentioned|Map legend|||||||||
17589|Sybella Granite|41298|6|Mentioned|Map legend|Carpentarian||||||||
17589|Sybella Granite|41465|6|Mentioned|p12|||||||||
17589|Sybella Granite|41791|6|Mentioned|p250|||||||||
17589|Sybella Granite|41862|6|Mentioned|p474|||||||||
17589|Sybella Granite|41958|6|Mentioned|p98|||||||||
17589|Sybella Granite|41978|6|Mentioned|Fig 2 P499|||||||||
17589|Sybella Granite|41979|6|Mentioned|p538|||||||||
17589|Sybella Granite|42367|4|Described|p18|||U-Pb zircon ages: 1610Ma and 1670Ma.||||||05-DEC-06
17589|Sybella Granite|42503|6|Mentioned|p334|||||||||
17589|Sybella Granite|42706|5|Briefly described|map legend|Paleoproterozoic|Palaeoproterozoic|Age: ~1670Ma. Biotite granite. commonly foliated and porphyritic.||||||09-FEB-09
17589|Sybella Granite|42830|6|Mentioned|p158|||||||||
17589|Sybella Granite|42879|6|Mentioned|p214|||||||||
17589|Sybella Granite|43607|6|Mentioned|p7|||||||||
17589|Sybella Granite|43608|6|Mentioned|Fig.11,p11|||||||||
17589|Sybella Granite|43760|6|Mentioned|p442|||||||||
17589|Sybella Granite|44210|14|Not recorded|p8-10,15|||||||||
17589|Sybella Granite|44257|14|Not recorded|p20,21|||Age: Rb-Sr.1540 Ma.||||||05-DEC-06
17589|Sybella Granite|44271|2|Defined|p41,46,48,52,53,60|||||||||
17589|Sybella Granite|44275|14|Not recorded|Map Legend|||||||||
17589|Sybella Granite|44290|14|Not recorded|p437|||||||||
17589|Sybella Granite|44309|2|Defined|Tb.1,opp.p7,map|||||||||
17589|Sybella Granite|44326|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
17589|Sybella Granite|44517|14|Not recorded|p234|||Intrudes Eastern Creek Volcanics and Judenan Beds.||||||
17589|Sybella Granite|44521|14|Not recorded|p14|||||||||
17589|Sybella Granite|44522|4|Described|p1,3-5,7,8,10-12|||Late Early Proterozoic.||||||05-DEC-06
17589|Sybella Granite|44552|14|Not recorded|p23|||||||||
17589|Sybella Granite|44751|14|Not recorded|p300||Precambrian|||||||
17589|Sybella Granite|44755|14|Not recorded|p91|||||||||
17589|Sybella Granite|44812|14|Not recorded|p7|||Soil.||||||
17589|Sybella Granite|44849|14|Not recorded|p69,74-5,82,87,94|||Age: 1780 Ma = approx age of Ewen Granite.||||||05-DEC-06
17589|Sybella Granite|44920|14|Not recorded|Map Legend, Sheet2,4||Carpentarian|||||||
17589|Sybella Granite|44989|2|Defined|p.149-152|||Tb.IV. = Templeton Group. (F54-1,5).||||||
17589|Sybella Granite|45003|14|Not recorded|p15,37|||||||||
17589|Sybella Granite|45052|5|Briefly described|p73|||K/Ar age||||||
17589|Sybella Granite|45072|6|Mentioned|p10|||Intrudes Eastern Creek. Volcanics.||||||05-DEC-06
17589|Sybella Granite|45079|6|Mentioned|p8|||Precambrian. Minimum age 1400 m.y.||||||
17589|Sybella Granite|45087|5|Briefly described|p14|||Chemical analyses.||||||
17589|Sybella Granite|45161|4|Described|p13|||||||||
17589|Sybella Granite|45166|5|Briefly described|p37|||||||||
17589|Sybella Granite|45287|14|Not recorded|p.228,231||Archean|||||||07-NOV-08
17589|Sybella Granite|46801|6|Mentioned|p115|||See also Fig. 14||||||
17589|Sybella Granite|46962|6|Mentioned|p251|||||||||
17589|Sybella Granite|46976|6|Mentioned|Fig.1|||||||||
17589|Sybella Granite|48894|6|Mentioned|p33|||Age. See also pp34,35,36.||||||05-DEC-06
17589|Sybella Granite|48906|14|Not recorded|p4,28|||||||||
17589|Sybella Granite|48997|6|Mentioned|Fig.3|||||||||
17589|Sybella Granite|49041|5|Briefly described|Table 1|||||||||
17589|Sybella Granite|50542|6|Mentioned|p96|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
17589|Sybella Granite|50550|5|Briefly described|p1140 Fig.3, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
17589|Sybella Granite|50624|6|Mentioned|236 Fig.3||Statherian|Sybella Batholith has age of 1660 Ma.||||||
17589|Sybella Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite granite.||||||
17589|Sybella Granite|60513|6|Mentioned|p281, p290, 288|||||||||
17589|Sybella Granite|61204|6|Mentioned|p544|Statherian|Statherian|Geological Province: Mount Isa Inlier. Age: ca. 1660 Ma (Page et al.,2000)||||||
17589|Sybella Granite|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: western Mount Isa Block.||||||07-NOV-08
17589|Sybella Granite|61736|5|Briefly described|p672 Fig. 7, p673|Paleoproterozoic|Paleoproterozoic|Age: 1671+/-8Ma. Geological province: Broken Hill Domain. Felsic magmatism.||||||24-FEB-10
17589|Sybella Granite|61922|5|Briefly described|p19 Fig. 11|||See also p21 Fig.13.||||||
17589|Sybella Granite|61923|5|Briefly described|p28 Fig.1|Paleoproterozoic|Paleoproterozoic|Comprises a suite of sheet-like bodies - a composite of intrusive phases, coarse-grained granodiorite to alkali-feldspar granite in this study area. Intrudes the Haslingden Group. Age: 1660+/-4 Ma and 1655+/-5 Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
17589|Sybella Granite|61924|6|Mentioned|p43B|||||||||
17589|Sybella Granite|61933|5|Briefly described|p169 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1675-1655 Ma; ca 1670-1655 Ma. See also p171 Tb.1.||||||07-NOV-08
17589|Sybella Granite|61936|5|Briefly described|p191, p194 Fig. 6|Mesoproterozoic|Paleoproterozoic|Age: ca 1610+/-13Ma, 1544+/-12Ma and 1510+/-13Ma.||||||07-NOV-08
17589|Sybella Granite|61963|6|Mentioned|p776|||Part of batholic plutons emplaced near Mount Isa.||||||
17589|Sybella Granite|62084|6|Mentioned|p950 Fig.14|||Mt Isa district.||||||
17589|Sybella Granite|62535|6|Mentioned|p672-673|Statherian|Statherian||1671 +/- 8 Ma.|||||
17589|Sybella Granite|62873|6|Mentioned|p692 Fig. 1|||||||||
17589|Sybella Granite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Coeval with Carters Bore Rhyolite.  Age: ~1675-1670Ma. Geological Province: Mount Isa Inlier.||||||07-NOV-08
17589|Sybella Granite|63023|5|Briefly described|p1024 Fig. 1, p1035|||Of Sybella Suite. Age: ca 1670Ma. Geological Province: Western Fold Belt.||||||
17589|Sybella Granite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|||||||
17589|Sybella Granite|63593|5|Briefly described|p285 Fig.1, p287, p288 Fig.2. |Palaeoproterozoic|Palaeoproterozoic|Western Fold Belt. 1600 km2. Appears as Sybella granite on p287. See also p291 Fig.3 and Tb.2.|ca. 1670 Ma|||Intrudes Carters Bore Rhyolite and McNamara Group.||
17589|Sybella Granite|64249|5|Briefly described|p82 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1675-1655Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
17589|Sybella Granite|64250|6|Mentioned|p8, p9 fig 1, p11 fig 3, p21-22|||Western Fold Belt, Mount Isa Inlier. Mention is also made of the Sybella Batholith, not a stratigraphic term.|1674 +/- 4 Ma - 1655 +/- 4 Ma.|||||
17589|Sybella Granite|64254|6|Mentioned|p171|||||||||
17589|Sybella Granite|64367|5|Briefly described|p555  Fig. 1b, p560, p561 Tb. 2|Paleoproterozoic|Paleoproterozoic|Of the Sybella Batholith. Age of batholith: 1675-1665Ma. Intruded the Eastern Creek Volcanics.||||||07-FEB-11
17589|Sybella Granite|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
17589|Sybella Granite|64726|6|Mentioned|p83 Fig.2.|||||||||
17589|Sybella Granite|64744|5|Briefly described|p353 Fig.4, p355 Fig.5, pp358-359.|Statherian|Statherian|Mount Isa Basin. A suite of stacked, I-type granite sill-like bodies, with amphibolite facies metamorphic aureole. Magmatism was synkinematic: gneissic fabric and near-identical monazite ages in the aureole.|1670 +/- 3 Ma.||||Granitic sills intercalated with lesser gabbro and dolerite.|
17589|Sybella Granite|64769|6|Mentioned|p26|Proterozoic|Proterozoic|QLD.||||||06-MAY-09
17589|Sybella Granite|64832|5|Briefly described|p1155 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Sybella Batholith which intruded the Haslingden Group. Age of emplacement: 1675-1655Ma (SHRIMP U-Pb zircon; Connors and Page 1995; Page et al 2000; Neumann et al 2005).||||||07-FEB-11
17589|Sybella Granite|64834|5|Briefly described|p13, p15, p32|||Sybella Intrusion shown in Fig.2|1678+/-8 Ma|||||
17589|Sybella Granite|65228|5|Briefly described|pp20-21, Fig.04.|Statherian|Statherian|Mount Isa region. Emplaced c.1680 - 1670 Ma.|1671 +/- 8 Ma.|||||
17589|Sybella Granite|65387|6|Mentioned|p55-56, p82|||A sample of migmatised gneissic granite, mapped as a component of this unit, was dated at 1782 +/- 5 Ma, but the authors point out that this sample is "different from other mapped units of the Sybella Batholith with which it has been equated".||||||05-APR-18
17589|Sybella Granite|65396|6|Mentioned|p11, p82, p103-104, p161, p172, p175|Statherian|Statherian|See also p193, p195, p241, p262, p274, p319, p361, p440. Lawn Hill Platform. Formations with detrital zircons from this unit are listed.|1675 +/- 3 Ma, 1660 +/- 5 Ma, 1655 +/- 4 Ma|||||
17589|Sybella Granite|65755|6|Mentioned|p2|||||||||
17589|Sybella Granite|66529|5|Briefly described|p3, p33, p37, p41, p94 |Proterozoic|Proterozoic|Western Mount Isa Province. Highly uranium enriched. ~1670 Ma Schofield (2009)||||||
17589|Sybella Granite|66824|5|Briefly described|p133-140, 145-151|||Referred to in the text as the Sybella Batholith (not a stratigraphic term); Wyborn (1979). Problems with previous age determinations discussed.|1660 +/- 5 Ma; 1655 +/- 4 Ma.|||Intrudes Haslingden Group.|An extensive felsic igneous complex, largely comprising granodiorite and alkali feldspar granite. Metamorphosed, multiply deformed, and metasomatised (detailed).|
17589|Sybella Granite|66844|6|Mentioned|p245|Statherian|Statherian|Mount Isa region. Age from SHRIMP dating.|1671+\-8 Ma|||||
17589|Sybella Granite|67127|6|Mentioned|p168|||Associated spatially with outcrops of the Mica Creek pegmatites [not a stratigraphic name].||||||
17589|Sybella Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.,p12|Paleoproterozoic|Paleoproterozoic|Sybella Igneous Event. Fractionated I-type granite.|1675 - 1670 Ma|Sybella Suite|||Foliated coarse-grained porphyritic biotite granite|
17589|Sybella Granite|67497|6|Mentioned|p905|||Mount Isa Inlier||||||
17589|Sybella Granite|67539|6|Mentioned|p8, p9 Fig.7|Statherian|Statherian|Sybella Belt. Contains xenolithic material with randomly oriented fabrics. Recent geochronology indicates that rocks intruded by the Sybella Granite in the southern Ardmore 1:100k Sheet area are not the Eastern Creek Volcanics as previously believed.|c. 1680 - 1670 Ma|||||
17589|Sybella Granite|68021|5|Briefly described|p135 fig 4, p136, p137, p138|Statherian|Statherian|Shown as Sybella granite p137.|1670 Ma|||Intrudes Eastern Creek Volcanics, Surprise Creek Formation.||
17589|Sybella Granite|68146|5|Briefly described|p1,p4,p6,p64, p106-112,p194,p201,p211|||Sybella Batholith, Mount Isa Region. Forms moderately well-exposed bouldery outcrops. Whole-rock Sm-Nd isotopic data tabulated.|1679 +/- 4 Ma.|||Adjacent to Big Toby Granite.|Pale orange, K-feldspar phyric (up to 3cm) foliated biotite granite.|
17589|Sybella Granite|68542|6|Mentioned|p10|||||||||
17589|Sybella Granite|68575|6|Mentioned|p53, p55|||At Yaringa Creek, along the W margin of the Sybella Batholith, the Big Toby Granite was mapped as this unit; the western edge of the Sybella Granite is farther east.||||||
17589|Sybella Granite|68576|5|Briefly described|QLD_D1: p5, p7, p17|||Near Mount Isa. Granite pavers of this unit are used in the Queen Street Mall.|||||Foliated porphyritic biotite granite with characteristic feldspar augen.|
17589|Sybella Granite|68732|5|Briefly described|p158 Fig.1, p165 Fig.3, p167, p168 Fig.5|Statherian|Statherian|Mount Isa Inlier. Igneous crystallisation ages.|1670 +/- 3, 1674 +/- 4, 1671 +/- 8 Ma|||||
17589|Sybella Granite|69222|6|Mentioned|p224 Fig.3, p225, p227|||Heat flow and production discussed; values given. Apperas as Sybella granite on p227.||||||
17589|Sybella Granite|69370|5|Briefly described|p306, p307 Fig.2 |Statherian|Statherian|Western Fold Belt, Mount Isa Block. Associated with rhyolites, dolerites, sandstones and mudstones of Cover Sequence 3. Age is 1671 Ma in Fig.1.|c.1680 Ma (Page and Bell, 1986).|||Intrudes Mount Isa and McNamara Groups.||25-JAN-19
17589|Sybella Granite|69542|6|Mentioned|p133 Fig.2, p134|Mesoproterozoic|Paleoproterozoic|Western Fold Belt. Mention is also made (p133) of the Sybella Batholith aged ~1665 Ma.||||||09-FEB-18
17589|Sybella Granite|69591|5|Briefly described|p32, p41-42, p59, p107|||Sybella Batholith. Coeval with extrusion of the Carters Bore Rhyolite.|1670 +/- 3 Ma (Neumann et al., 2006).|||Is surrounded by (?intrudes) Alpha Centauri Metamorphics.|Strongly foliated coarse-grained porphyritic biotite granite.|
17589|Sybella Granite|70283|5|Briefly described|p25 Fig.1|Paleoproterozoic|Paleoproterozoic|The Sybella batholith term seems to be preferred in this article; it intrudes the Haslingden Group, was emplaced at 1660 +/- 4 Ma to 1655 +/- 5 Ma, and is broadly contemporaneous with the Mount Isa Group.|||||Granite.|14-FEB-18
17589|Sybella Granite|70858|6|Mentioned|p29, 31, 33|Paleoproterozoic|Paleoproterozoic|Tommy Creek Block, Isan Superbasin. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.|1.67 Ga.|||||
17589|Sybella Granite|70897|6|Mentioned|p41|||Source of 1680 Ma zircons in Mullera Formation.||||||
17589|Sybella Granite|71369|6|Mentioned|p4|||||||||
17589|Sybella Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen. Both ages are crystallisation: U-Pb zircon SHRIMP.|1795+/-5 Ma and 1679+/-4 Ma.||||Granite.|
17589|Sybella Granite|72297|5|Briefly described|p702, p726|||Near Mount Isa. Used as dimension stone; its granite tiles, slabs and stone pave the Queen Street Mall in Brisbane. The beryl crystal-bearing Mica Creek Pegmatite is a phase of this unit.||||||
17589|Sybella Granite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. 6 ages given as U-Pb zircon igneous crystallisation ages. Range shown in age field.|1679 +/-4 Ma to 1655 +/-4 Ma|||||
17589|Sybella Granite|72889|5|Briefly described|p23-25.|Statherian|Statherian|Of Sybella Batholith. Four previous magmatic ages reported from Neumann et al. 2006, and Carson et al.2011. [Age with smallest error indexed].|1669.7+/-2.9 Ma|||Co-magmatic with dolerite reported herein.||
17589|Sybella Granite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Six U-Pb zircon igneous crystallisation ages (Ma) shown. Oldest and youngest recorded here.|1679 +/- 4 Ma to 1655 +/- 4 Ma|||Shown as overlying Carters Bore Rhyolite and underlying McNamara Group.||
17589|Sybella Granite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a series of 6 U-Pb zircon igneous crystallisation ages (see Fig.1.2 for list of dates).|~1655+/-4 to1679+/-4 Ma|||||
17589|Sybella Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
17605|Sylvester Sandstone|10116|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Silicified quartzose sandstone, green siltstone.||||||
17605|Sylvester Sandstone|22954|6|Mentioned|Fig3p9|||||||||
17605|Sylvester Sandstone|30914|6|Mentioned|Map legend|Early Cambrian|Proterozoic|Proterozoic - Early Cambrian||||||
17605|Sylvester Sandstone|31287|6|Mentioned|p430|||||||||
17605|Sylvester Sandstone|33111|6|Mentioned|p38|||||||||
17605|Sylvester Sandstone|34454|5|Briefly described|Table 2|||L.Cambrian||||||
17605|Sylvester Sandstone|34847|6|Mentioned|p31|||||||||
17605|Sylvester Sandstone|35121|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17605|Sylvester Sandstone|35139|4|Described|Table.2|||||||||
17605|Sylvester Sandstone|36234|3|Fully described|p166|||||||||
17605|Sylvester Sandstone|36243|6|Mentioned|Table 1A|||||||||
17605|Sylvester Sandstone|37572|5|Briefly described|p155|||See also Fig.8||||||
17605|Sylvester Sandstone|39445|5|Briefly described|Table 4|||See also p62.||||||05-DEC-06
17605|Sylvester Sandstone|39921|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Early to Middle CambrianE - M||||||
17605|Sylvester Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
17605|Sylvester Sandstone|42956|5|Briefly described|p31 Fig.4|||||||||
17605|Sylvester Sandstone|44121|14|Not recorded|p5|Early Cambrian|Neoproterozoic|||||||
17605|Sylvester Sandstone|44211|14|Not recorded|p97,102|||||||||
17605|Sylvester Sandstone|44291|14|Not recorded|p8|||||||||
17605|Sylvester Sandstone|44308|14|Not recorded|p3,5,Tb.1||Early Cambrian|Equivalent to Mount Birnie Beds.||||||
17605|Sylvester Sandstone|44312|14|Not recorded|Map Legend||Early Cambrian|||||||
17605|Sylvester Sandstone|44543|2|Defined|p31,32,36||Early Cambrian|Overlies Sun Hill Arkose. No fossils.||||||
17605|Sylvester Sandstone|44920|14|Not recorded|Map Legend, Sheet 4||Adelaidean|||||||
17605|Sylvester Sandstone|45052|3|Fully described|p75|||Adelaidean||||||
17605|Sylvester Sandstone|47058|6|Mentioned|Fig.8 P129|||||||||
17605|Sylvester Sandstone|49027|6|Mentioned|p3|||Mention p5.||||||05-DEC-06
17605|Sylvester Sandstone|63450|5|Briefly described|p78 Fig. 5, p80|Cambrian|Cambrian|Geological province: Georgina Basin, East Toko Syncline.||||||07-FEB-11
17605|Sylvester Sandstone|64068|3|Fully described|p54, 55, 225|Early Cambrian|Early Cambrian|360 m thick in type section. Presumed to be Cambrian but may be Neoproterozoic. Correlations: Mount Baldwin Formation, Adam Shale and Red Heart Dolostone (Shergold 1985: 7).||Of Shadow Group.||Presumed to unconformably overlie Sun Hill Arkose.|Silicified brown sandstone, green siltstone.|04-APR-12
17605|Sylvester Sandstone|65489|5|Briefly described|p125|Cambrian|Cambrian|Georgina Basin.||||Overlies Mount Birnie Beds and Sun Hill Arkose. Is overlain unconformably by Thorntonia Limestone.||
17605|Sylvester Sandstone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Early Cambrian|Neoproterozoic|East Toko Syncline, Georgina Basin.||Shadow Group.||Is overlain by Thorntonia Limestone.|Conglomerate, arenite, arkose, shale, mudstone, dolomite.|
17605|Sylvester Sandstone|67870|6|Mentioned|p43|Early Cambrian|Early Cambrian|Georgina Basin.||||||
17605|Sylvester Sandstone|68270|5|Briefly described|p681,683|Early Cambrian|Early Cambrian|Southern Georgina Basin.||||Underlain unconformably by Sun Hill Arkose.||
17605|Sylvester Sandstone|69443|5|Briefly described|p28:7, 14-15|Early Cambrian|Early Cambrian|Southern Georgina Basin.||Shadow Group.||Possible correlative of Octy, Neutral Junction and Mount Baldwin Formations.||12-JUL-16
17605|Sylvester Sandstone|69591|5|Briefly described|p87, p94|Cambrian|Cambrian|West Toko Syncline, Georgina Basin. The rather complicated history of interpretation of this unit is given.||||Overlies Sun Hill Arkose. Is overlain transitionally by Thorntonia Limestone.|Silicified sandstone and green siltstone.|
17605|Sylvester Sandstone|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation.||02-JUN-21
17630|Tabor Gabbro|30692|6|Mentioned|Map legend|Miocene|Oligocene|Miocene to Oligocene||||||
17630|Tabor Gabbro|39445|5|Briefly described|Table 14|||||||||
17630|Tabor Gabbro|43982|14|Not recorded|Map Legend||Tertiary|||||||
17630|Tabor Gabbro|43994|14|Not recorded|Map Legend||Tertiary|||||||
17630|Tabor Gabbro|44022|14|Not recorded|Map Legend||Tertiary|||||||
17630|Tabor Gabbro|44023|4|Described|Tb.2,p13||Tertiary|||||||
17630|Tabor Gabbro|44337|5|Briefly described|Map Legend||Tertiary|Lithology.||||||
17630|Tabor Gabbro|45071|3|Fully described|Table 15|||||||||
17630|Tabor Gabbro|45110|4|Described|p122|||||||||
17630|Tabor Gabbro|48919|5|Briefly described|p76|||Tertiary||||||
17630|Tabor Gabbro|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as the Silver Plains Nephelinite, Mount Barney Central Complex, Mount Jukes Intrusive Complex, and unnamed basaltic to rhyolitic plugs, are all mapped under the symbol, Ti.||||||
17630|Tabor Gabbro|69599|6|Mentioned|p637|||About 60km SW of the Buckland volcano.||||||
17664|Talban Granite|31659|6|Mentioned|p86|||Refers Mt. Morgan Ltd Staff (1965)||||||
17664|Talban Granite|44370|14|Not recorded|p218|||||||||
17666|Talbot Creek Granodiorite|9539|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Grey, pink and cream biotite leucogranodiorite with sporadic muscovite; minor pegmatite.||||||
17666|Talbot Creek Granodiorite|23291|5|Briefly described|p33|||Defined by Withnall et al, 1976. Replaced by Talbot Creek Trondhjemite. Geological Province: Georgetown Region.||||||19-MAY-15
17666|Talbot Creek Granodiorite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17666|Talbot Creek Granodiorite|33909|2|Defined|p230|Proterozoic|Proterozoic|||||||
17666|Talbot Creek Granodiorite|35214|6|Mentioned|p7|||||||||
17666|Talbot Creek Granodiorite|37570|4|Described|p119|||||||||
17666|Talbot Creek Granodiorite|39445|5|Briefly described|Table 2|||See also P45||||||
17666|Talbot Creek Granodiorite|39687|6|Mentioned|p3|||||||||
17666|Talbot Creek Granodiorite|50198|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
17666|Talbot Creek Granodiorite|50199|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
17666|Talbot Creek Granodiorite|50595|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Muscovite-biotite trondhjemite.||||||01-JUL-04
17666|Talbot Creek Granodiorite|68352|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, cream or pink, medium- to coarse-grained muscovite-biotite trondhjemite.|
17666|Talbot Creek Granodiorite|68353|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, cream or pink, medium- to coarse-grained muscovite-biotite trondhjemite.|08-JUL-15
17666|Talbot Creek Granodiorite|68354|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Forsayth Batholith, Etheridge Province.|||||Grey, cream or pink, medium- to coarse-grained muscovite-biotite trondhjemite.|08-JUL-15
17666|Talbot Creek Granodiorite|69591|6|Mentioned|p82|Mesoproterozoic|Mesoproterozoic|Withnall et al. (1976). Subsequently the Talbot Creek Trondhjemite.||||||
17685|Talgai Pedoderm|42593|5|Briefly described|p301|||||||||
17685|Talgai Pedoderm|69600|5|Briefly described|p661|Pleistocene|Pleistocene|Sobbe (1990). A unit in limited stratigraphies of sections along creeks in the eastern Darling Downs. Not considered to be a valid stratigraphic unit.||||||
17835|Tararan Basalt|42895|3|Fully described|p73|||Pliocene age. Variation on Tararan Melanephelinite?||||||
17835|Tararan Basalt|61155|5|Briefly described|p20|Late Pliocene|Early Pliocene|Overlain by Berrembea, Barambah and Hummock Basalts. In the Bundaberg-Maryborough region.||||||
17835|Tararan Basalt|68421|5|Briefly described|Map Legend|Piacenzian|Piacenzian|Bundaberg Volcanic Province. K-Ar (anorthosite) ages (Robertson, 1992).|2.69 +/- 0.09 Ma, 2.99 +/- 0.06 Ma.||||Olivine nephilinite, analcime nephelinite, basanite, hawaiite and mugearite.|
17850|Tareela Volcanics|23422|5|Briefly described|p180, p205 Table 6.3|Carboniferous|Early Carboniferous|Of Glenrock Group.||||||
17850|Tareela Volcanics|23430|5|Briefly described|p506|||Of Glenrock Group. Burdekin Basin Province.||||||
17850|Tareela Volcanics|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Glenrock Group.||||||
17850|Tareela Volcanics|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V61.||||||
17850|Tareela Volcanics|23893|5|Briefly described|p17|Namurian|Visean|Of Glenrock Group.  Geological Province: Kennedy Province.||||||
17850|Tareela Volcanics|24612|5|Briefly described|p9 Fig.2|Early Carboniferous|Early Carboniferous|Geological Province: Burdekin Basin.||||||06-APR-05
17850|Tareela Volcanics|24613|2|Defined|p6 Fig. 3, p68, p102-103|Early Carboniferous|Early Carboniferous|Of Glenrock Group. Contains Ponto Basalt Member and Eridge Member. Overlies Keelbottom Group rocks. Geological province: Burdekin Basin. Lithology comprises three informal units and two members. Rhyolite, basalt, andesite - detailed lithology included.||||||07-FEB-11
17850|Tareela Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17850|Tareela Volcanics|32169|6|Mentioned|Table 2|||U.Carb.||||||
17850|Tareela Volcanics|32553|4|Described|p46|||||||||
17850|Tareela Volcanics|34408|6|Mentioned|p185|||On Table||||||
17850|Tareela Volcanics|36472|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
17850|Tareela Volcanics|37573|6|Mentioned|p226|||See also Fig.2||||||
17850|Tareela Volcanics|37613|6|Mentioned|p249|||See also Fig.3||||||
17850|Tareela Volcanics|39445|5|Briefly described|Table 7|||||||||
17850|Tareela Volcanics|39686|6|Mentioned|p73|||||||||
17850|Tareela Volcanics|39735|6|Mentioned|p18|||||||||
17850|Tareela Volcanics|41774|6|Mentioned|p32|||||||||
17850|Tareela Volcanics|41916|5|Briefly described|p31|||||||||
17850|Tareela Volcanics|42295|5|Briefly described|Fig.2 P5|||||||||
17850|Tareela Volcanics|42407|6|Mentioned|p13|||||||||
17850|Tareela Volcanics|42547|4|Described|p77|||||||||
17850|Tareela Volcanics|42689|5|Briefly described|map legend|Carboniferous||||||||
17850|Tareela Volcanics|42933|6|Mentioned|p225|||||||||
17850|Tareela Volcanics|43095|1|Redefined|p22|Early Carboniferous||||||||
17850|Tareela Volcanics|43259|4|Described|Appendix 1,p6.||Early Carboniferous|||||||
17850|Tareela Volcanics|43589|1|Redefined|p18|Early Carboniferous|Early Carboniferous|North Queensland Volcanic and Plutonic Province (NQVP). Formerly included in the Glenrock Group (Hutton et al 1994).||||||23-APR-08
17850|Tareela Volcanics|44060|14|Not recorded|Map Legend||Late Carboniferous|||||||
17850|Tareela Volcanics|44061|4|Described|Table 3||Late Carboniferous|||||||
17850|Tareela Volcanics|45097|6|Mentioned|p22|||No control on age. See also correlation chart||||||
17850|Tareela Volcanics|45151|5|Briefly described|Table 7|||||||||
17850|Tareela Volcanics|46845|6|Mentioned|Table 1|||||||||
17850|Tareela Volcanics|48904|2|Defined|p41|Late Carboniferous|Late Carboniferous|||||||
17850|Tareela Volcanics|68419|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.||Of the Glenrock Group.|Includes the Eridge Volcanic Member and Ponto Basalt Member.||Mafic and felsic lavas and volcaniclastic rocks.|
17850|Tareela Volcanics|68420|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Burdekin Basin.||Of the Glenrock Group.|Includes the Eridge Volcanic Member and Ponto Basalt Member.||Rhyolite, rhyolitic to andesitic ignimbrites, tuffs, breccia, basalt and andesite.|
17850|Tareela Volcanics|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit, as well as the Butlers, Cumberland Range, Maureen and Sundown Volcanic Groups; parts of the Featherbed, Newcastle Range and Scardons Volcanic Groups; the Bally Knob, Nanyeta, Pratt, Reamba and Saint Giles Volcanics; the Hells Gate, Oweenee, Paluma, Porcupine Creek and Watershed North Rhyolites; and the Paddock Creek Formation, are all mapped under the symbol, Cvk.||||||
17850|Tareela Volcanics|68731|5|Briefly described|p187|||Gunther and Withnall (1992). Occupies a northwest bounded fault block on ROLLINGSTONE named the Tareela Graben. < 2500 m thick.|||Includes the Eridge Member and the Ponto Member.|Disconformably underlain by the Keelbottom Group.|Lower: felsic breccia, ash and lapilli tuff, flow-banded rhyolite and ignimbrite. Upper: aphyric to porphyritic basalt and andesite flows, with some andesitic breccia and lapilli tuff.|
17850|Tareela Volcanics|69593|5|Briefly described|p495-496|Visean|Visean|Charters Towers region; Broken River Province.||Glenrock Group.|||Includes basaltic and andesitic lava, rhyolitic ignimbrite, tuff and pyroclastic rocks.|
17861|Tarong beds|12597|6|Mentioned|p498|Triassic|Triassic|||||||
17861|Tarong beds|13516|6|Mentioned|p159 fig 8, p164|Late Triassic|Late Triassic|From Tarong area, Clarence-Moreton Basin.||||||
17861|Tarong beds|23799|3|Fully described|p43, p10 Tb. 1, p48 Fig. 3|Late Triassic|Late Triassic|The only strat. unit in Tarong Basin - derived from erosion of Boondooma Igneous Complex and metasediments of the Maronghi Creek beds.  Intruded by younger phases of Boondooma Igneous Complex.  Overlain by Main Range Volcanics.  Geol. Prov: Tarong Basin.||||||15-APR-13
17861|Tarong beds|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
17861|Tarong beds|24560|5|Briefly described|Map legend|Late Triassic|Late Triassic|||||||
17861|Tarong beds|39943|6|Mentioned|Table 12A|||||||||
17861|Tarong beds|40486|6|Mentioned|p82|||||||||
17861|Tarong beds|40487|6|Mentioned|p77|||||||||
17861|Tarong beds|40488|6|Mentioned|p92|||||||||
17861|Tarong beds|42187|6|Mentioned|p319|||||||||
17861|Tarong beds|42492|5|Briefly described|p12|||||||||
17861|Tarong beds|43001|5|Briefly described|p127|||||||||
17861|Tarong beds|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Tarong Basin.||||||12-APR-05
17861|Tarong beds|44923|5|Briefly described|Map Legend||Late Triassic|||||||
17861|Tarong beds|50320|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Tarong Basin (Wandilla Province).||||||09-JUN-04
17861|Tarong beds|50384|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Tarong Basin||||||
17861|Tarong beds|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Tarong Basin. Sandstone, shale, coal, conglomerate||||||
17861|Tarong beds|60371|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Tarong Basin. Sandstone, shale, coal, conglomerate||||||
17861|Tarong beds|61002|5|Briefly described|p209|Late Triassic|Late Triassic|||||||
17861|Tarong beds|64665|5|Briefly described|p53 Fig.2, p57, p62.|Late Triassic|Late Triassic|Tarong Basin. Coal-bearing alluvial fan deposits. Sediment provenance was from the west; shows fining-upward trend on a macro scale. Seam splitting is common. High ash, high volatile bituminous rank.||||Unconformably overlies Boondooma Igneous Complex in the west.|Conglomerates, finer clastics, coal.|
17861|Tarong beds|67402|4|Described|p239, p258, p259|Rhaetian|Carnian|Tarong Basin. Unsuitable reservoir for the storage of carbon dioxide.Up to 450m thick. Deposited as alluvial fans, fluvial deposits and flood-basin deposits.|||||Sandstone, pebbly sandstone, conglomerate, siltstone, coal and mudstone.|
17861|Tarong beds|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Tarong Basin.||||||
17861|Tarong beds|68679|5|Briefly described|p322-323, p388, p396-399|Late Triassic|Late Triassic|Tarong Basin. >300m thick. Alluvial fans, fluvial swamp and lacustrine environments. Complex and rapid lateral and vertical variations make it impossible to recognise mappable stratigraphic units.||||Unconformably overlies Maronghi Creek beds and Sugarloaf Metamorphics. Correlated with Ipswich Coal Measures.|Thin, grey carbonaceous shale; labile, poorly sorted, fine- to coarse-grained, poorly bedded or lensoidal sandstone; granule to pebble conglomerate with labile sandstone matrices. At least five coal seams (to 35m thick).|
17861|Tarong beds|69582|5|Briefly described|p82, p84, p86|||Sole unit of the Tarong Basin. These units are excellent geothermal insulators. Preserved thickness is estimated at 450m.||||Unconformably overlies the Maronghi Creek beds.|Sandstone, siltstone, mudstone and coal.|
17861|Tarong beds|69594|6|Mentioned|p519|||Tarong Basin.||||||
17861|Tarong beds|72297|5|Briefly described|p698, p700|Triassic|Triassic|Tarong Basin; 190km NW of Brisbane. 450m thick. Coeval with Tivoli Formation, and slightly older than the Callide Coal Measures. Coal is extracted at the Meandu mine for the Tarong power station. Other potentially mineable deposits mentioned.|||King seam, Queen seam.||Mainly sandstone and conglomerate, with at least six coal seams. The coal is high-ash (unsuitable for export), low-sulfur, high-volatile bituminous rank.|
17882|Tasman Formation|38445|6|Mentioned|p105|||||||||
17882|Tasman Formation|39495|6|Mentioned|p142|||||||||
17901|Tawah Granodiorite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
17901|Tawah Granodiorite|39445|5|Briefly described|Table 12|||||||||
17901|Tawah Granodiorite|40475|6|Mentioned|Table 2|||||||||
17901|Tawah Granodiorite|45440|2|Defined|p.60,78||Triassic|Tb.1. 215 + 5 m yrs.||||||
17901|Tawah Granodiorite|63821|5|Briefly described|p31|Late Triassic|Late Triassic|Age: 220Ma (K-Ar biotite).  Comprises hornblende tonalite, hornblende quartz diorite to hornblende-pyroxene diorite, biotite granite and muscovite-biotite granite.||||||07-FEB-11
17901|Tawah Granodiorite|68679|5|Briefly described|p430|||Ellis (1968); subsequently the Tawah Granite (Cranfield and Murray, 1989) but apparently has reverted to its original name (Denaro et al., 2007), although Tawah Granite is given priority (and bold type) in this study.|221 Ma (K-Ar: Webb and McDougall, 1967).|||Intrudes the Gympie Group.|Hornblende tonalite, hornblende quartz diorite to hornblende-pyroxene diorite, perthitic biotite granite, muscovite-biotite granite and hornblende-biotite granite; relative proportions are unknown.|
17902|Tawallah Group|7071|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|22432|5|Briefly described|p20|||In the McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22453|5|Briefly described|p 11|||||||||
17902|Tawallah Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
17902|Tawallah Group|22538|4|Described|P707, P714|Statherian|Orosirian|Part of the Redbank package||||||06-JUN-18
17902|Tawallah Group|22644|5|Briefly described|3,4,7,9,12,13|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22664|6|Mentioned|35|Paleoproterozoic|Paleoproterozoic|Geological province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|22665|6|Mentioned|P222|||||||||
17902|Tawallah Group|22670|6|Mentioned|53,54,56,58,59,60|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22673|6|Mentioned|64|||Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|22853|4|Described|5|Proterozoic|Proterozoic|Geol province McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23066|5|Briefly described|p807, Fig.1|Proterozoic|Proterozoic|Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23195|6|Mentioned|p5|||Informally referred to "Upper" Tawallah Group.||||||
17902|Tawallah Group|23197|6|Mentioned|Fig.1, p850|||Informally referred to as lower and upper Tawallah Group.||||||
17902|Tawallah Group|23374|6|Mentioned|p8,41,42,34,6,8,30||Statherian|Equivalent to Kombolgie Subgroup. Geological province: McArthur Basin.||||||11-DEC-06
17902|Tawallah Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23395|4|Described|p384 Fig.2|||||||||
17902|Tawallah Group|23396|5|Briefly described|p407 Fig.2|||||||||
17902|Tawallah Group|23397|6|Mentioned|p471|||||||||
17902|Tawallah Group|23398|5|Briefly described|p436|Statherian|Statherian|||||||
17902|Tawallah Group|23406|5|Briefly described|p601 Fig.3|||||||||
17902|Tawallah Group|23407|5|Briefly described|p627 Fig.2|||||||||
17902|Tawallah Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
17902|Tawallah Group|23776|5|Briefly described|p704|||||||||
17902|Tawallah Group|23809|5|Briefly described|p27|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Tomkinson Creek Group (Ashburton Province) and Birrindudu Group (Birrindudu Basin), and the Wauchope and Hanlon Subgroups of Hatches Creek Group (Davenport Province).||||||
17902|Tawallah Group|23867|5|Briefly described|p14|||See also Fig. 30.  Geological  Province: McArthur Basin.||||||
17902|Tawallah Group|23910|4|Described|p290|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|23937|6|Mentioned|p4 Fig. 4, p51|||||||||
17902|Tawallah Group|23963|4|Described|p1237, 1239 Fig.2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin. Age: 1857+/-30 Ma. Overlies the Scrutton Volcanics.||||||07-NOV-08
17902|Tawallah Group|23968|6|Mentioned|p1346 Fig. 1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: 1800-1700Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|24048|6|Mentioned|p6|||Geological Province: McArthur Basin||||||
17902|Tawallah Group|24050|6|Mentioned|p12|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|24197|6|Mentioned|p54|||Contains igneous suites of rocks which are either bimodal, dominantly felsic or dominantly mafic. Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Includes Hobblechain Rhyolite, Selgal Volcanics and Westmoreland Conglomerate.   Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
17902|Tawallah Group|24432|6|Mentioned|p559|||||||||
17902|Tawallah Group|30272|6|Mentioned|p5|||On stratigraphic table||||||
17902|Tawallah Group|30318|6|Mentioned|p327|||||||||
17902|Tawallah Group|30344|6|Mentioned|p29|||See also Fig.4||||||
17902|Tawallah Group|30345|6|Mentioned|Table 1|||Carpentarian age. Lithology||||||
17902|Tawallah Group|30508|6|Mentioned|p94|||Stratigraphy||||||
17902|Tawallah Group|30534|6|Mentioned|p306|||||||||
17902|Tawallah Group|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|31824|6|Mentioned|p28|||Middle Proterozoic||||||
17902|Tawallah Group|32339|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32479|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|32519|6|Mentioned|p340|||||||||
17902|Tawallah Group|32658|4|Described|Table 2|||See also Fig.3||||||
17902|Tawallah Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|32660|4|Described|Table 4|||||||||
17902|Tawallah Group|32904|6|Mentioned|p89|||||||||
17902|Tawallah Group|33214|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|33665|5|Briefly described|p366|||||||||
17902|Tawallah Group|34287|6|Mentioned|p34|||||||||
17902|Tawallah Group|34754|6|Mentioned|p15|||||||||
17902|Tawallah Group|35114|6|Mentioned|p203|||||||||
17902|Tawallah Group|35162|6|Mentioned|p1007|||||||||
17902|Tawallah Group|35261|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|35495|6|Mentioned|p340|||||||||
17902|Tawallah Group|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|35776|6|Mentioned|p814|||See also Table 1.||||||
17902|Tawallah Group|35950|6|Mentioned|p311|||||||||
17902|Tawallah Group|36012|3|Fully described|Table 2|||||||||
17902|Tawallah Group|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17902|Tawallah Group|37217|6|Mentioned|p650|||||||||
17902|Tawallah Group|37372|6|Mentioned|p2|||||||||
17902|Tawallah Group|37462|4|Described|Table4.IV|||||||||
17902|Tawallah Group|37565|5|Briefly described|p3|||See also Fig.5.||||||11-DEC-06
17902|Tawallah Group|37568|4|Described|p75|||||||||
17902|Tawallah Group|37569|6|Mentioned|p91|||||||||
17902|Tawallah Group|38042|6|Mentioned|p160|||||||||
17902|Tawallah Group|38156|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|38529|6|Mentioned|p275|||||||||
17902|Tawallah Group|38582|6|Mentioned|p215|||||||||
17902|Tawallah Group|38584|4|Described|p10|||||||||
17902|Tawallah Group|38902|6|Mentioned|p20|||||||||
17902|Tawallah Group|39122|6|Mentioned|p154|||||||||
17902|Tawallah Group|39210|5|Briefly described|p50|||||||||
17902|Tawallah Group|39445|6|Mentioned|p36|||See also p39.||||||11-DEC-06
17902|Tawallah Group|39497|6|Mentioned|Fig.4|||||||||
17902|Tawallah Group|39561|6|Mentioned|Fig.5|||||||||
17902|Tawallah Group|39685|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|39925|6|Mentioned|p337|||||||||
17902|Tawallah Group|40105|6|Mentioned|p310|||See also Fig.7||||||
17902|Tawallah Group|40109|5|Briefly described|p302|||||||||
17902|Tawallah Group|40259|6|Mentioned|Table 1|||||||||
17902|Tawallah Group|40489|6|Mentioned|p89|||||||||
17902|Tawallah Group|40491|6|Mentioned|p79|||||||||
17902|Tawallah Group|40691|3|Fully described|p7|||||||||
17902|Tawallah Group|40840|6|Mentioned|Map legend|||||||||
17902|Tawallah Group|40973|6|Mentioned|p193|||||||||
17902|Tawallah Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|41019|5|Briefly described|p243|||||||||
17902|Tawallah Group|41125|6|Mentioned|p35|||||||||
17902|Tawallah Group|41220|5|Briefly described|p366|||||||||
17902|Tawallah Group|41268|4|Described|p283|||||||||
17902|Tawallah Group|41277|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|41319|6|Mentioned|Fig.1|||||||||
17902|Tawallah Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41721|3|Fully described|p8|||Comprises 10 named units and is the oldest group in the McArthur Basin sequence. Overlies igneous and metamoprhic complexes of the Murphy Inlier; disconformably overlain by Masterton Sandstone. Geological province: McArthur Basin.||||||01-AUG-07
17902|Tawallah Group|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|41957|6|Mentioned|p68|||||||||
17902|Tawallah Group|42385|3|Fully described|p5|Paleoproterozoic|Paleoproterozoic|Includes Yiyintyti Sst, Seigal Volc, Sly Creek Sst, Aquarium Fm, Wununmantyala Sst, Settlement Creek Volcs, Wollogorang Fm, Gold Creek Volcs, Warramana Sst and Tanumbirini Rhyolite. Age between 1857 +/- 30Ma and 1725 +/- 40 Ma. Composite thickness: >5km.||||||06-JUN-18
17902|Tawallah Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
17902|Tawallah Group|42395|6|Mentioned|Fig.26 P86|||||||||
17902|Tawallah Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||10 fm, 1 mbr. Yiyintyi Ss, Seigal Volcs, Sly Creek Ss (Rosie Creek Ss Mbr), Aquarium Fm, Wununmantyala Ss, Settlement Ck Volcs, Wollogorang Fm, Gold Ck Volcs, Warramana Ss, Tanumbirini Rhyolite.|Underlies McArthur Group.||06-OCT-11
17902|Tawallah Group|42639|3|Fully described|p8, Table 4 p11|Mesoproterozoic||||||||
17902|Tawallah Group|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
17902|Tawallah Group|42739|5|Briefly described|map legend|Statherian|Statherian|Quartz sandstone, conglomerate, mudstone, basaltic and rhyolitic volcanics, minor dolostone.||||||19-OCT-05
17902|Tawallah Group|42753|6|Mentioned|p2|||||||||
17902|Tawallah Group|42812|4|Described|p10, Table 3|||||||||
17902|Tawallah Group|42846|5|Briefly described|p503|||Geological Province: McArthur Basin.||||||09-MAY-05
17902|Tawallah Group|42873|5|Briefly described|p109|||see also Fig.1, p110.||||||11-DEC-06
17902|Tawallah Group|42935|5|Briefly described|p527|||||||||
17902|Tawallah Group|43010|6|Mentioned|p91|||of "Mid Proterozoic" age.||||||
17902|Tawallah Group|43036|4|Described|p13|||||||||
17902|Tawallah Group|43107|6|Mentioned|p9|||||||||
17902|Tawallah Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|43595|4|Described|p438||Mesoproterozoic|||||||
17902|Tawallah Group|43615|6|Mentioned|p14|||||||||
17902|Tawallah Group|43788|6|Mentioned|p13||Proterozoic|||||||
17902|Tawallah Group|44112|6|Mentioned|p10,43|||Part of Supersequence 1(B); middle and upper units in 1(C); upper units in 1(D)||||||
17902|Tawallah Group|44155|6|Mentioned|p252|||McArthur Basin. Probable part correlative of Mount Parker Sandstone and Bungle Bungle Dolomite.||||||
17902|Tawallah Group|44287|14|Not recorded|p.6-16|||(E53-3).||||||
17902|Tawallah Group|44288|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44299|6|Mentioned|p.11|||SD/53-7,8.||||||
17902|Tawallah Group|44305|14|Not recorded|p.11-13,18|||(E53-8). opp.p.6,18.||||||
17902|Tawallah Group|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44332|14|Not recorded|p.7,11,12,opp.6,map|||(D53-14).||||||
17902|Tawallah Group|44333|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44434|14|Not recorded|opp.p.6,map|||Correlated with Groote Eylandt Beds. (D53-11,12).||||||
17902|Tawallah Group|44435|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
17902|Tawallah Group|44436|5|Briefly described|p.6-10,opp.p.7,map|||(E53-4).||||||02-DEC-04
17902|Tawallah Group|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Includes the Masterton, Wollogorang and Aquarium Formations, and the Settlement Creek Volcanics.||||||07-NOV-08
17902|Tawallah Group|44459|14|Not recorded|p.6,7,opp.p.6, map|||(E53-2). Here includes Rosie Creek Sandstone, Settlement Creek Volcanics, Wollogorang Formation, Masterton Formation (top). See p.12,13, for more details.||||||
17902|Tawallah Group|44460|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44471|14|Not recorded|p.7|||(D53-10).||||||
17902|Tawallah Group|44473|14|Not recorded|p.7-8,13-15,opp. p.7|||(E53-7).||||||
17902|Tawallah Group|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|44482|14|Not recorded|p.7|||(E53-12).||||||
17902|Tawallah Group|44530|14|Not recorded|p.4-17|||(D53-15).||||||
17902|Tawallah Group|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
17902|Tawallah Group|45032|14|Not recorded|p9||Carpentarian|Tb.1, Pl.1.||||||
17902|Tawallah Group|45140|6|Mentioned|p12-13|||McArthur Basin region.|~1575 Ma.|||||
17902|Tawallah Group|45162|2|Defined|p11|Proterozoic|Proterozoic|||||||
17902|Tawallah Group|45166|6|Mentioned|p14|||||||||
17902|Tawallah Group|45167|5|Briefly described|Fig.27|||||||||
17902|Tawallah Group|46804|6|Mentioned|p154|||||||||
17902|Tawallah Group|46861|6|Mentioned|p2|||||||||
17902|Tawallah Group|46915|6|Mentioned|Fig.1|||Stratigraphic section through McArthur Group.||||||
17902|Tawallah Group|46955|6|Mentioned|p159|||||||||
17902|Tawallah Group|46968|6|Mentioned|Fig.2|||||||||
17902|Tawallah Group|49001|6|Mentioned|p4|||||||||
17902|Tawallah Group|50225|5|Briefly described|p407|||Geological Province: McArthur Basin.||||||07-FEB-11
17902|Tawallah Group|50591|5|Briefly described|p1.1|||Geological Province: McArthur Basin.||||||
17902|Tawallah Group|60483|4|Described|p6, p7 Fig. 5|Paleoproterozoic|Paleoproterozoic|Unconformable over basement units including Scrutton Volcanics, and McArthur Group. Max.age: ~1850Ma; min.age: 1713+/-7Ma. Geol.Prov: McArthur Basin. Dominated by shallow marine to fluvial sandstone, with lesser mudstone, dolostone, igneous rocks.||||||07-NOV-08
17902|Tawallah Group|60558|5|Briefly described|p7, p8 Fig. 6, p10, p12|Proterozoic|Proterozoic|Includes 14 units. Coarse-grained terrigenous to shallow marine clasticsand mafic volcanics, with lesser shallow water to shelf carbonates.||||||
17902|Tawallah Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17902|Tawallah Group|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
17902|Tawallah Group|62084|6|Mentioned|p956||||||||Mafic and felsic volcaniclastic rocks, clastic and minor volcanic rocks.|
17902|Tawallah Group|62285|6|Mentioned|p380, p381|||||||||
17902|Tawallah Group|63110|6|Mentioned|p1141|||Includes; Settlement Creek and Gold Creek Volcanics. Overlain by McArthur Group.||||||11-JUN-08
17902|Tawallah Group|63112|6|Mentioned|p1190, p1992 Tb.1 |||Southern McArthur Basin. Also includes Warramana, Wununmantyala, Rosie Creek, Sly Creek, Echo and Yiyintyi Sandstones and Westmoreland Conglomerate.|||Includes Tanumbirini, Hobblechain Rhyolites; Packsaddle Microgranite; Gold Creek, Settlement Creek, Seigal  Volcanics; Aquarium, McDermott, Nyanantu, Wollogorang Formations. NB: See Comments.|||
17902|Tawallah Group|63866|5|Briefly described|p112, p115|||Southern McArthur Basin.||||Equivalent to the Katherine River Group and the Spencer Creek Group.||
17902|Tawallah Group|64250|6|Mentioned|p25 fig 10|||Southern McArthur Basin. Contemporaneous with volcanism in Mount Isa Inlier.|~1795-1695 Ma.||Includes Seigal Volcanics, Gold Creek Volcanics.|||15-MAR-18
17902|Tawallah Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Lower part of this group of the Leichhardt Superbasin (McArthur Basin), deposited during the Leichhardt Extension (1800-1750 Ma). Upper part is part of the Calvert Superbasin, deposited during the Calvert Event (~1730-1690 Ma).||||||
17902|Tawallah Group|64815|5|Briefly described|p3, p4 Fig.2, p5 Fig.3, p6, p10-13|Statherian|Orosirian|See also p15 Fig.9, p16-18 Figs.10-12. Represents the Redbank package. The topmost units are often missing in stratigraphic successions. Appears as Subgroup in Figs.10-12.|Deposition from 1815-1705 Ma.||Includes Yiyintyi, Sly Creek, Warramana, Wununmantyala Sandstones; Seigal, Settlement Creek, Gold Creek, Volcanics; Aquarium, Wollogorang, Nyanantu Formations; Tanumbirini Rhyolite.|Unconformably overlies Scrutton Volcanics.|Composed of sandstone, with bimodal igneous intrusions and lavas, lutite, conglomerate and dolostone.|
17902|Tawallah Group|64817|5|Briefly described|p352 Fig.3, p353 Fig.4, p354, 355, 357|||Also includes Tanumbirini and Hobblechain Rhyolite; Gold Creek, Settlement Creek and Seigal Volcanics. A mid-Tawallah Group east-west compressional event deformed and uplifted older units of the Group.|Shown as ~1790 - <1705 Ma.||Includes Burash, Echo, Warramana, Wununmantyala, Sly Creek and Yiyintyi Sandstones; Westmoreland Conglomerate; Nyanantu, Wollogorang, Aquarium and McDermott Formations; and various volcanic units.|||06-JUN-18
17902|Tawallah Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
17902|Tawallah Group|65228|4|Described|p7, p19, Fig.02|||McArthur Basin. c.5,000 m thick. Lower parts of this unit comprise the Leichhardt Superbasin. Also includes Hobblechain and Tanumbirini Rhyolites.|||Includes Yiyintyi, Sly Creek, Wununmantyala, Warramana Sandstones; Seigal, Settlement Creek, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang Formations; Westmoreland Conglomerate and others.||Shallow water clastics; minor carbonate, shale and volcanic rocks.|
17902|Tawallah Group|65232|5|Briefly described|p9, p20, p78|||Includes Westmoreland Conglomerate at base, Seigal Volcanics, and Wollogorang Formation. Correlatives of Katherine River Group and Tolmer Group. Unconformably overlie northern margin of Murphy Inlier. Uranium deposits. Geol. Prov: McArthur Basin.||||||09-FEB-10
17902|Tawallah Group|65337|6|Mentioned|p6 Fig.3, p15.|||McArthur Basin. Correlative of Carrara Range Group.||||||
17902|Tawallah Group|65340|3|Fully described|p5,  p.13 Table 4, pp11-57, p 66.|||PhD thesis and related papers published (Rawlings 1998, 1999, 2002). Oldest, most areally extensive and voluminous unit in southern McArthur Basin. Forms a regionally extensive, mainly flat-lying platform 2.5 to 6 km thick. Resistant sandstone ranges and plateaux; very little deformation is due to its zone of tectonic stability as well as the structurally competent, thick homogeneous sandstone packages. Probably contiguous with Katherine River Group, Tennant Creek Inlier and Mount Isa Inlier. Contemporaneous with Katherine River, Donydji and Spencer Creek Groups.|||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Burash and Echo Sandstones; Seigal, Gold Creek and other Volcanics; McDermott, Wollogorang and Nyanantu Formations; and more.|Unconformably overlies Murphy and Scrutton Inliers. Is unconformably overlain by McArthur Group,and Karns Dolomite.|Dominated by shallow-marine and fluviatile sandstone, with lesser mudstone, dolostone and bimodal (basalt-rhyolite) volcanic and high-level intrusive rocks.|23-MAR-18
17902|Tawallah Group|66529|5|Briefly described|p21 |||||||Overlies Seigal Volcanics.|Dolomite, sandstone and mafic and felsic volcanic rocks.|
17902|Tawallah Group|66843|5|Briefly described|p23-24|||Oldest tectonic-stratigraphic package in the southern McArthur Basin.|1760 - 1710 Ma.|||Is overlain unconformably by McArthur Group.|Mainly quartz-rich sandstones and mafic to felsic igneous rocks.|
17902|Tawallah Group|67144|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.|||Includes Westmoreland Conglomerate; Seigal, Settlement Creek and Gold Creek Volcanics; McDermott and Wollogorang Formations; Sly Creek Sandstone.|Is overlain by McArthur Group.||13-APR-12
17902|Tawallah Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p107|||CONSTITUENTS (continued): Gold Creek, Seigal, Settlement Creek, Cliffdale Volcanics.|||Aquarium, McDermott, Wollogorang Formations; Carolina Sandstone Member; Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; Hobblechain Rhyolite. See COMMENTS for more.|||
17902|Tawallah Group|67352|4|Described|v, p11-12, p14-15 Tb.2, p50|Statherian|Statherian|McArthur Basin (Calvert Superbasin). Up to 6 km thick.|1790-1705 Ma||Includes Gold Creek Volcanics, Wollogorang Formation, Settlement Creek Volcanics, Sly Creek Sandstone, McDermott Formation and Seigal Volcanics.|Overlain by McArthur Group (unconformably).|Shallow-marine to fluviatile sandstone and volcanigenic and shallow-intrusive rocks, together with minor lutite, conglomerate and dolostone.|08-JAN-15
17902|Tawallah Group|67564|6|Mentioned|p86.|||Southern McArthur Basin.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|67779|5|Briefly described|p32, p36.|||Southern McArthur Basin. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Spencer Creek Group, Gadabara Volcanics, Groote Eylandt Group and Donji Group.|||Includes Sly Creek Sandstone.|||
17902|Tawallah Group|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|McArthur Basin, Mount Isa Province.||||Is overlain conformably by Peters Creek Volcanics.||
17902|Tawallah Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
17902|Tawallah Group|69418|6|Mentioned|p3:15||||||Gold Creek Volcanics.|||12-JUL-16
17902|Tawallah Group|69423|5|Briefly described|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Settlement Creek dolerite, Seigal Volcanics, Westmoreland Conglomerate.|||12-JUL-16
17902|Tawallah Group|69429|5|Briefly described|p14:3|||McArthur Basin.|||Yiyintyi Sandstone.|Unconformably overlies Scrutton Volcanics.||12-JUL-16
17902|Tawallah Group|69430|4|Described|p15:2-4, 9-14, 35, 39, 62|||Southern McArthur Basin. Also includes igneous units: Settlement Creek Dolerite; Hobblechain, Tanumbirini Rhyolites; Packsaddle Microgranite. Generally shallow dipping or flat-lying. May be contiguous with Tomkinson Creek Group (Tomkinson Creek Province) and Haslingden Group (Isa Superbasin). Mentioned as a source of metals for the McArthur River Zn-Pb-Ag deposit. Hosts a number of small U-Au deposits surrounding the Murphy Inlier (described in detail).|>1710 Ma.||Westmoreland Conglomerate; Yiyintyi, Sly Creek, Wununmantyala, Warramana, Echo, Burash Sandstones; Seigal, Gold Creek Volcanics; McDermott, Aquarium, Wollogorang, Nyanantu Formations.|Is overlain unconformably by the McArthur and Nathan Groups. Is correlated, and probably contiguous, with the Katherine River Group.|Shallow-marine and fluvial sandstone, with lesser mudstone, dolostone and mafic and felsic volcanic rocks, and coeval and younger intrusive bodies.|12-JUL-16
17902|Tawallah Group|69433|6|Mentioned|p18:1-2, 10|||McArthur Basin.||||Equivalent to Wire Creek Sandstone and Peters Creek Volcanics (Lawn Hill Platform).||12-JUL-16
17902|Tawallah Group|69591|5|Briefly described|p29, p39, p56, p58|Paleoproterozoic|Paleoproterozoic|Camooweal-Murphy Domain, Mount Isa Province. The only unit in the McArthur Basin succession N of the Murphy Tectonic Ridge in Qld.|||Westmoreland Conglomerate; Sly Creek, Wire Creek Sandstones; McDermott, Aquarium, Wollogorang Formations; Gold Creek, Seigal, Settlement Creek Volcanics; Hobblechain Rhyolite.|||
17902|Tawallah Group|69673|4|Described|p15, p17, p20, p22, p32, p40, p49, p51|Statherian|Statherian|Also includes Tanumbirini Rhyolite, Warramana Sandstone, Hobblechain Rhyolite, Gold Creek Volcanics, Wollogorang Formation, Settlemenet Creek Dolerite, Wununmantyala Sandstone, Aquarium Formation, McDermott Formation, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|1710 Ma||Includes Burash Sandstone, Nyanantu Formation, Echo Sandstone|Correlated with Birrindudu Group|Extensively silicified arkosic or quartz rich sandstone that alternate with mafic volcanic rocks, shale and rare carbonate rocks.|
17902|Tawallah Group|70284|5|Briefly described|p1245|Statherian|Statherian|Leichhardt Superbasin. 1000-4000m thick. Age inferred from age of Leichhardt Superbasin.|||||Fluvial conglomeratic sandstones, mafic volcanics and marine and aeolian sediments.|
17902|Tawallah Group|70302|5|Briefly described|iv, p7|Statherian|Statherian|Southern McArthur Basin. Age is also derived from Page and Sweet, 1998.|c.1730 Ma (Page et al., 2000).|||Correlated with Woodah Sandstone.||05-FEB-18
17902|Tawallah Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic|Chronostratigraphy is adapted from Brasier and Lindsay (1998) and Southgate et al. (2000).|1729 +/- 4 Ma to 1713 +/- 7 Ma.|||Overlain by McArthur Group||06-JUN-18
17902|Tawallah Group|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin and 'Tawallah Group equivalent' on Lawn Hill Platform. Also includes Packsaddle Microgranite.|||Wire Creek, Sly Creek Sandstones; Peters Creek, Seigal, Settlement Creek, Gold Creek Volcanics; Westmoreland Conglomerate; McDermott, Aquarium, Wollogorang Formations; Hobblechain Rhyolite.|Unconformably overlies Murphy Metamorphics and Cliffdale Volcanics.|Conglomerate, sandstone, greywacke, dolostone; basalt, dolerite, rhyolite, rhyodacite, dacite, trachyte, microgranite.|21-FEB-18
17902|Tawallah Group|70968|6|Mentioned|p2 Fig.3|||||||||
17902|Tawallah Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
17902|Tawallah Group|71374|5|Briefly described|p2, p6|||southern McArthur Basin.|||Includes the Gold Creek Volcanics, Wollogorang Formation and Wununmantyala Sandstone.|Unconformably overlain by the McArthur Group. Equivalent to the lower Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups.||
17902|Tawallah Group|71606|5|Briefly described|p135,137|Statherian|Statherian|Bauhinia Shelf, Batten Trough and Wearyan Shelf, McArthur Basin. Arenite-bimodal volcanic-lutite-carbonate sequence. Age is constrained by 1710-1700 Ma Fagan Phase.|||Includes Hobblechain and Tanumbirini Rhyolites.|Correlable to Groote Eylandt Group. Overlain unconformably by Nathan and McArthur groups, and Karns Dolomite. Correlable to Katherine River Group.||
17902|Tawallah Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Informally subdivided into lower and upper parts.||||||06-MAR-20
17902|Tawallah Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Quartz sandstone with lesser conglomerate, dolostone, fine-grained clastics, and mafic and felsic volcanics.|
17902|Tawallah Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Redbank package, and Spencer Creek, Groote Eylandt, Donydji, Katherine River and Edith River groups (northern McArthur Basin), Birrindudu and Tolmer groups (Birrindudu Basin) and Tomkinson Creek and Hatches Creek groups (Tomkinson Province).||||||
17902|Tawallah Group|72377|5|Briefly described|iii,p12|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Wollogorang Formation and Tanumbirini Rhyolite.|||
17902|Tawallah Group|72523|6|Mentioned|p1.|Palaeoproterozoic|Palaeoproterozoic|||||Unconformably underlies the  Nathan Group.||
17902|Tawallah Group|72526|5|Briefly described|p4, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana,  Sandstone, Echo, Wununmantyala, Sly Ck. and Yiyintyi Ss, Nyanantu, Wollogorang, Aquarium and McDermott Fms, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics, Cliffdale Volcanics and Nicholson Granite Complex and unconformably underlying McArthur Group.||
17902|Tawallah Group|72527|6|Mentioned|p1, p3, p5, p7, p176, 185, 193, 194.|Paleoproterozoic|Paleoproterozoic|This group is divided by an unconformity between the earlier Wire Creek Sandstone and Peters Creek Volcanics. Lithographically also contains rounded clasts of predominantly white vein quartz, quartzite, felsic volcanics and rarely, granite.|||Includes Peters Creek Volcanics and Wire Creek Sandstone|Shown as laterally equivalent to and unconformably underlying Carrara Range Group and partially and unconformably overlying Murphy Metamorphics.|Includes feldspathic coarse and coarse-grained, gritty quartz sst., occasionally cross-bedded, with pebble lags and local cobble to boulder congl. lenses.|
17902|Tawallah Group|72718|6|Mentioned|piii, p5, p7|Palaeoproterozoic|Palaeoproterozoic|Beetaloo Sub-basin, McArthur Basin. Calvert/Leichhardt Superbasin, Redbank package. More constituents include the Tanumbirini and Hobblechain rhyolites, Packsaddle Microgranite, Gold Creek and Seigal volcanics, and the Settlement Creek Dolerite.|||Burash, Echo, Warramana, Wununmantyala, Sly Creek, Yiyintyi sandstones; Nyanantu, Wollogorang, Aquarium, McDermott formations; Westmoreland Conglomerate [see comments].|Conformably overlain by Parsons Range Group. Unconformably overlain by McArthur River Group,Nathan Group, Roper Group.|Dominated by shallow-marine to fluvial sandstone, with lesser shale, conglomerate, dolostone and bimodal volcanic rocks.|
17902|Tawallah Group|72912|4|Described|p5 Fig.3, p18-19, p36, p48.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin. Age constraints from dating of basal Westmoreland Conglomerate at 1815+/-7 Ma (sedimentary depositional age) and Tanumbirini Rhyolite, near top at 1713+/-7 Ma. This group also includes Settlement Creek Dolorite and Westmoreland Conglomerate.|||Burash, Warramana, Echo, Wununmantyala, Sly Creek and Yiyintyi Sandstones, Nyanantu, Wollogorang, Aquarium and McDermott Formations, Tanumbinini, Hobblechain Rhyolites, Gold Creek, Seigal Volcanics,|Shown as unconformably overlying Scrutton Volcanics and partially Westmoreland Conglomerate. Shown as unconformably underlying Umbolooga Subgroup, McArthur Group.|Includes sandstone, conglomerate, rhyolite and dolerite.|
17902|Tawallah Group|72919|6|Mentioned|p3, p12|Paleoproterozoic|Paleoproterozoic||||Westmoreland Conglomerate|||
17902|Tawallah Group|72967|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|||||||
17902|Tawallah Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert and Leichhardt Superbasin. Constituents: Burash Sandstone, Echo Sandstone, Nyanantu Formation, Tanumbinini Rhyolite, Warramana Sandstone, Pungalina Member, Hobblechain Rhyolite, Gold Creek Volcanics, Settlement Creek Dolorite, Wununmantyala Sandstone, Wuraliwuntya Member, Aquarium Formation, McDermott Formation, Rosie Creek Sandstone Member, Sly Creek Sandstone, Seigal Volcanics, Yiyintyi Sandstone, Westmoreland Conglomerate.|||See comments.|||
17902|Tawallah Group|73083|6|Mentioned|p35, p37, p40|Paleoproterozoic|Paleoproterozoic||||Seigal Volcanics||Includes a basal sandstone.|
17902|Tawallah Group|73412|4|Described|p1-2, 4, 6-20|||Southern McArthur Basin. Dry bulk density tabulated. Essentially flat-lying stratigraphy. Faults described. Low gravity response; magnetic response is high where volcanic units are preserved; non-conductive unit. Exposed at the surface c.10 km W of the Emu Fault Zone. Mafic volcanics are thought to be the source of Zn and Pb.|1790-1700 Ma.||Yiyintyi Sandstone, Westmoreland Conglomerate, Seigal Volcanics, Wununmantyala Sandstone, Wollogorang Formation, Settlement Creek and Gold Creek Volcanics.|Is overlain unconformably by McArthur Group.|Widespread fluvial to intertidal sandstones and conglomerates and an anomalously thick (c.2 km) pile of mafic volcanics; overlain by shallow marine siliciclastics and carbonates, and volcanics.|
17919|Teddy Mount Formation|23032|5|Briefly described|p33|Early Carboniferous|Late Devonian|||||||
17919|Teddy Mount Formation|23424|4|Described|Table 8.1 p337.|Early Carboniferous|Late Devonian|Age: Latest Devonian to Early Carboniferous (latest Famennian to Tournaisian); conodonts and brachiopods. Of Bundock Creek Group, Bundock Basin. Maximum thickness 1420 m.||||||18-JUN-13
17919|Teddy Mount Formation|23430|5|Briefly described|Plate 14.11 + p510|||Also see p507. Of Bundock Creek Group. Graveyard Creek Subprovince.||||||
17919|Teddy Mount Formation|23431|5|Briefly described|p541|||||||||
17919|Teddy Mount Formation|24613|6|Mentioned|p77, p135|Late Devonian|Late Devonian|Part of the upper Bundock Creek Group. Geological province: Broken River Province,  Graveyard Creek Subprovince.||||||18-JUN-13
17919|Teddy Mount Formation|41260|3|Fully described|p90|||Reserved as Teddy Mountain Formation.||||||08-MAY-15
17919|Teddy Mount Formation|41679|6|Mentioned|Fig.2|||||||||
17919|Teddy Mount Formation|41719|6|Mentioned|Fig.2|||||||||
17919|Teddy Mount Formation|41739|2|Defined|p301|Tournaisian|Famennian|||||||
17919|Teddy Mount Formation|41740|6|Mentioned|p222|||||||||
17919|Teddy Mount Formation|42054|6|Mentioned|p273|||||||||
17919|Teddy Mount Formation|42693|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
17919|Teddy Mount Formation|42709|6|Mentioned|map legend|||||||||
17919|Teddy Mount Formation|42933|3|Fully described|p169|||of Bundock Creek Group||||||
17919|Teddy Mount Formation|43286|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|of Bundock Creek Group.||||||
17919|Teddy Mount Formation|43603|5|Briefly described|p9|||||||||
17919|Teddy Mount Formation|50200|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Bundock Creek Group.||||||
17919|Teddy Mount Formation|64707|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|Of Bundock Creek Group. Fine- to medium-grained, micaceous, feldspathic sandstone, mudstone and minor impure limestone; local marine fossils.||||||
17919|Teddy Mount Formation|65214|6|Mentioned|p280|Devonian|Devonian|QLD, Broken River. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17919|Teddy Mount Formation|67402|4|Described|p239, p245 |Tournaisian|Famennian|Bundock Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited in a marginal marine to shallow marine/shelfal environment. Maximum thickness of 1420m.||||Overlies the Turrets Formation. Overlain by the Boroston Formation.|Feldspathic to lithofeldspathic sandstone and minor dirty limestone.|
17919|Teddy Mount Formation|68297|5|Briefly described|p186, 194, 195|Famennian|Late Devonian|Broken River embayment. Include Late Devonian vertebrate fossil assemblages in a limestone member.||||||
17919|Teddy Mount Formation|68336|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|Includes Dyraaba Member.||Fine- to medium-grained, micaceous, feldspathic sandstone, mudstone and minor impure limestone; local marine fossils.|07-MAY-15
17919|Teddy Mount Formation|68338|5|Briefly described|Map legend.|Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|||Fine- to medium-grained, micaceous, feldspathic sandstone, mudstone, and minor impure limestone; local marine fossils.|
17919|Teddy Mount Formation|68341|5|Briefly described|Map legend.|Early Carboniferous|Late Devonian|Graveyard Creek Subprovince.||Unit in Bundock Creek Group.|Includes Dyraaba Member.||Fine- to medium-grained, micaceous, feldspathic sandstone, mudstone and minor impure limestone; local marine fossils.|07-MAY-15
17919|Teddy Mount Formation|68410|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably overlain by the Boroston Formation. Conformably underlain by the Turrets Formation.|Fine to medium-grained, micaceous, feldspathic sandstone, mudstone and minor dirty limestone; local marine fossils.|
17919|Teddy Mount Formation|68478|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably underlain by the Turrets Formation.|Fine to medium-grained, micaceous, feldspathic sandstone, mudstone and minor impure limestone; local marine fossils.|
17919|Teddy Mount Formation|68479|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Bundock Basin.||Of the Bundock Creek Group.||Conformably underlain by the Turrets Formation.|Fine to medium-grained, micaceous, feldspathic sandstone, mudstone and minor impure limestone; local marine fossils.|
17919|Teddy Mount Formation|69030|5|Briefly described|p6|Carboniferous|Carboniferous|Bundock Basin (Broken River Province).||Bundock Creek Group.||||
17919|Teddy Mount Formation|69592|4|Described|p259, p272 Fig.4.61, p273-274, p276|Late Devonian|Late Devonian|Bundock Basin, Broken River Province. >1400m thick; distributed across the entire Basin. Contains abundant macrofauna and microfauna, and horizons with plant debris. Shallow-marine to paralic environments.||Bundock Creek Group.|Dyraaba Member.|Conformably overlies Turrets Formation. Is overlain conformably by Boroston Formation.|Fossiliferous mudstone, siltstone and fine-grained sandstone with subordinate impure limestone. Sandstone is commonly cross-stratified, burrowed, feldspathic to lithofeldspathic, generally calcareous and characterised by detrital muscovite.|
17921|Teebar Formation|24382|5|Briefly described|Map legend|Permian|Permian|Parent: Gympie Group.||||||14-AUG-08
17921|Teebar Formation|41736|2|Defined|p119|Late Permian||Reserved as Teebar||||||
17921|Teebar Formation|41778|6|Mentioned|Fig.2|||||||||
17921|Teebar Formation|42054|6|Mentioned|p272|||||||||
17921|Teebar Formation|43017|5|Briefly described|Fig.3,p375|||||||||
17921|Teebar Formation|63821|4|Described|p17|Late Permian|Late Permian|Topmost unit of the Gympie Group. Intruded by Mount Urah Granodiorite. Geological Province: Gympie Province. Comprises medium- to coarse-grained sandstone, conglomerate, siltstone and mudstone of marginal marine to continental environments.||||||07-FEB-11
17921|Teebar Formation|68679|5|Briefly described|p370|Wuchiapingian|Wuchiapingian|Northern Gympie Province. From Gigoomgan homestead S to the Munna mine. 200m thick.||||Correlated with Tamaree Formation.|Sandstone, siltstone, carbonaceous shale, rhythmically bedded turbidites dominated by volcanic lithic fragments with rare conglomerates; cross-bedding, load casts and flame structures common; poorly fossiliferous.|
17921|Teebar Formation|73303|4|Described|p61 Fig.2, p62-64, p66 Fig.6, p67-69|Lopingian|Lopingian|New England Orogen. Gympie Terrane, northern. Individual bed-sets typically have basal erosive margins, normal grading, flat lamination and upper wavy lamination or hummocky cross-stratification. Trace fossils include Arenacolites, Rhizocorallium and Thallassanoides. ca 254 Ma detrital zircon maximum depositional age. Shallow marine shelf depositional environment with sediment derived from Carboniferous sources in New England Orogen.|257-252 Ma, ca 254 Ma detrital zircon|||Conformably overlies Gigoomgan Limestone, underlies Brooweena Formation.|Rhythmically bedded marine siliciclastic sandstone-siltstone beds. Predominantly medium-bedded, well-sorted, medium- to fine-grained cream sandstone interbedded with thick- to medium-bedded siltstone. Coarsens upwards in uppermost part.|
17932|Telemon Formation|22540|6|Mentioned|Fig.1 p778|Dinantian|Late Devonian|||||||
17932|Telemon Formation|22800|5|Briefly described|p583, Fig.8 p587|||||||||
17932|Telemon Formation|23161|6|Mentioned|p13|||||||||
17932|Telemon Formation|23184|6|Mentioned|Fig1p178|Hastarian||||||||
17932|Telemon Formation|23430|6|Mentioned|p510|||||||||
17932|Telemon Formation|23522|5|Briefly described|p250 Fig 6|Early Carboniferous|Late Devonian|||||||
17932|Telemon Formation|24075|5|Briefly described|p394 Fig. 2|Early Carboniferous|Late Devonian|Lithic and feldspathic sandstone, conglomerate, siltstone and mudstone; minor lithic sandstone and mudstone.  2100m.  Geological Province: Drummond Basin.||||||
17932|Telemon Formation|30546|6|Mentioned|p107|||Correlation||||||
17932|Telemon Formation|30691|4|Described|p12|||See also P13,Table 3. Upper Devonian To Lower Carboniferous||||||
17932|Telemon Formation|30814|2|Defined|p68|Early Carboniferous|Late Devonian|Late Devonian to Early Carboniferous.||||||21-OCT-08
17932|Telemon Formation|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
17932|Telemon Formation|32490|6|Mentioned|p7|||See also P8||||||
17932|Telemon Formation|32493|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17932|Telemon Formation|32865|6|Mentioned|p483|||Carb.||||||
17932|Telemon Formation|33092|5|Briefly described|p7|||Strat. table||||||
17932|Telemon Formation|33096|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17932|Telemon Formation|33645|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17932|Telemon Formation|33646|6|Mentioned|p9|||Strat. table.||||||
17932|Telemon Formation|34085|6|Mentioned|Cor.chart|||Famennian||||||
17932|Telemon Formation|34174|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
17932|Telemon Formation|34389|4|Described|Table 1|||Upper Devonian - Lower Carboniferous||||||
17932|Telemon Formation|34390|4|Described|Table 1|||Upper Devonian||||||
17932|Telemon Formation|34392|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Upper Devonian - Lower Carboniferous||||||
17932|Telemon Formation|35811|5|Briefly described|Table 4|||||||||
17932|Telemon Formation|35913|6|Mentioned|p35|||||||||
17932|Telemon Formation|37451|6|Mentioned|Table 2|||||||||
17932|Telemon Formation|38374|6|Mentioned|p599|||||||||
17932|Telemon Formation|38527|6|Mentioned|p306|||||||||
17932|Telemon Formation|39445|5|Briefly described|Table 6|||||||||
17932|Telemon Formation|39813|6|Mentioned|Map legend|Late Devonian|Late Devonian|Prob.Upper Devonian||||||
17932|Telemon Formation|40623|5|Briefly described|p110|||||||||
17932|Telemon Formation|41120|5|Briefly described|p196|||||||||
17932|Telemon Formation|41246|6|Mentioned|Map legend|Carboniferous||||||||
17932|Telemon Formation|42547|5|Briefly described|Fig.17 P61|||||||||
17932|Telemon Formation|42614|4|Described|P 9|||Drummond Basin||||||
17932|Telemon Formation|42701|6|Mentioned|p25|||||||||
17932|Telemon Formation|43029|5|Briefly described|p24|||||||||
17932|Telemon Formation|43204|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin||||underlies Mount Hall Formation||23-DEC-11
17932|Telemon Formation|43213|4|Described|p69, p78, p91-92, p94, p238|Early Carboniferous|Early Carboniferous|Drummond Basin. First described by Shell (Queensland) Development Pty Ltd (1952) and Hill (1957), and later by Veevers et al. (1964) and Olgers (1972). Possibly equivalent to Glendarriwell beds. Contains common lepidodendroids. Up to 1050m thick. Geophysics described.||||Overlies Silver Hills Volcanics.|Mainly olive-green mudstones and shales, with thick interbeds of green and grey sandstone and minor conglomerate. Includes quartzose sandstone.|
17932|Telemon Formation|43461|14|Not recorded|p616-7,Table p618|Early Carboniferous|Late Devonian|||||||
17932|Telemon Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
17932|Telemon Formation|43990|14|Not recorded|Map Legend|Carboniferous|Late Devonian|||||||
17932|Telemon Formation|43994|14|Not recorded|Map Legend|||||||||
17932|Telemon Formation|43998|4|Described|p20,map|Carboniferous|Devonian|||||||
17932|Telemon Formation|43999|14|Not recorded|p95,,96||Middle Devonian|||||||
17932|Telemon Formation|44010|14|Not recorded|p68,69|||||||||
17932|Telemon Formation|44051|14|Not recorded|Fig.25,opp.p178|||||||||
17932|Telemon Formation|44070|14|Not recorded|p141||Late Devonian|Unconformably overlies Dunstable Formation.||||||
17932|Telemon Formation|44081|4|Described|p30,38-41,46-8,62-4,|||p73,75-6,79,109,112,133,Fig.7,154,,158,160-8,173,187,198,Pl.8. Described in French.||||||
17932|Telemon Formation|44085|2|Defined|Opp.p4-6,14,15,map|||||||||
17932|Telemon Formation|44091|14|Not recorded|p33,39,Tb.3,p46|Carboniferous|Devonian|||||||
17932|Telemon Formation|44102|14|Not recorded|p175-176|||||||||
17932|Telemon Formation|44331|14|Not recorded|Map Legend|Early Carboniferous|Late Devonian|||||||
17932|Telemon Formation|44337|5|Briefly described|Map Legend||Early Carboniferous|Lithology.||||||
17932|Telemon Formation|45071|3|Fully described|Table 1|||||||||
17932|Telemon Formation|45073|4|Described|p27|||Measured section P30,31||||||
17932|Telemon Formation|45097|6|Mentioned|Fig.|||Carboniferous. Correlation chart||||||
17932|Telemon Formation|46849|6|Mentioned|Fig. 2|||||||||
17932|Telemon Formation|46881|6|Mentioned|Table 2|||||||||
17932|Telemon Formation|48843|14|Not recorded|p.8,14,16|Carboniferous|Devonian|(F55-11).||||||
17932|Telemon Formation|48845|2|Defined|p6-11,13,16,18-20,||Late Devonian|p23-27,Fig.10,map. Overlies Silver Hills Volcanics. Overlain by Mount Hall Conglomerate.||||||
17932|Telemon Formation|48900|3|Fully described|p11|||Upper Devonian and possibly Lower Carboniferous.||||||
17932|Telemon Formation|48908|6|Mentioned|p21|Carboniferous|Devonian|||||||
17932|Telemon Formation|48915|6|Mentioned|Table 1|||Devonian - Carboniferous||||||
17932|Telemon Formation|48920|3|Fully described|p19|||Upper Devonian to Lower Carboniferous. Part of Drummond Group.||||||21-OCT-08
17932|Telemon Formation|48951|6|Mentioned|Table 1|||||||||
17932|Telemon Formation|60369|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Overlies the Silver Hills Volcanics. Lithic conglomerate and sandstone, mudstone, algal limestone, minor agglomerate, tuff, rhyolite.||||||02-SEP-04
17932|Telemon Formation|61394|5|Briefly described|p964 Fig. 1|Tournaisian|Tournaisian|Geological Province: southern Drummond Basin.||||||04-OCT-05
17932|Telemon Formation|64315|5|Briefly described|p510 Tb. 1|Early Carboniferous|Late Devonian|Max. thickness: 2100m. Geological province: southern Drummond Basin. Quartzose sandstone, conglomerate, shaley siltstone; concretionary and algal limestone bands in upper section.||||||
17932|Telemon Formation|65214|6|Mentioned|p282|Devonian|Devonian|NSW, Telemon. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17932|Telemon Formation|66188|6|Mentioned|Fig 3|Early Carboniferous|Early Carboniferous|Drummond Basin||||||
17932|Telemon Formation|67402|5|Briefly described|p165 tbl LPB1, p197, p201 tbl DRM2|||Drummond Basin. Deposited on a floodplain.|||||Siltstones and mudstones.|
17932|Telemon Formation|68297|5|Briefly described|p187, 197|Tournasian|Fammenian|Qld. Includes chondrichthyan shark teeth. Includes Early Carboniferous vertebrate fauna.||||||
17932|Telemon Formation|68326|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Drummond Basin||||Is overlain conformably by Mount Hall Formation.|Lithic sandstone and conglomerate, siltstone, algal limestone and minor tuffaceous siltstone.|02-DEC-13
17932|Telemon Formation|68414|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Drummond Basin. Map symbol (Ct) indicates that unit isconsidered Carboniferous.||||Conformably overlain by the Mount Hall Formation. Conformably underlain by the Foyle Volcanics.|Lithic sandstone and conglomerate, siltstone, algal limestone, and minor tuffaceous siltstone.|29-AUG-14
17932|Telemon Formation|68482|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Drummond Basin.||||Conformably overlain by the Mount Hall Formation.|Lithic sandstone and conglomerate, siltstone, algal limestone and minor tuffaceous siltstone.|
17932|Telemon Formation|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. This unit, as well as the Mount Hall and Scartwater Formations and Raymond Sandstone, are all mapped under the symbol, Cd2.||||||
17932|Telemon Formation|68731|5|Briefly described|p172, p173, p191 Fig 3.102|Mississippian|Mississippian|Drummond Basin. Crops out in the Telemon, Nogoa and Mount Beauford anticlines. Plant remains are uncommon and are non-diagnostic of age, as are rare fish scales and ostracods (Olgers 1972).||||Conformably overlain by the Mount Hall Formation.|Comprises a lower conglomerate and pebbly sandy unit, as well as an upper unit of quartzose to lithic, planar to cross-laminated sandstone interbedded with varicoloured mudstone and hard red siltstone.|18-JUL-14
17932|Telemon Formation|68900|3|Fully described|p4, p37, p52, p54-57, p62, p64, p66|Carboniferous|Carboniferous|Drummond Basin. The name was first used by SQD (1952) and Hill (1957) and is the basal unit of Cycle 2 in the southern Drummond Basin. Crops out in the cores of the Telemon and Nogoa Anticlines and along the eastern margin of the Drummond Basin. No type area has been specified, although Olgers (1972) illustrated a measured section north-east of Withersfield. This unit generally forms recessive topography, particularly in relation to over and underlying units. This unit generally has a low response in radiometric and magnetic images. Interpreted to have been deposited in a fluvial-lacustrine environment. In the Nogoa Anticline this unit is 2100m thick. Biostratigraphy is discussed in detail.||||Overlain by the Mount Hall Formation. Disconformably overlain by the Raymond Formation. Disconformably (to unconformably) overlies the Foyle Volcanics. Overlies the Silver Hills Volcanics.|Cross-bedded conglomerate, conglomeratic sandstone, fine-grained sediments and limestone.|
17932|Telemon Formation|69599|6|Mentioned|p593|||||||Is overlain unconformably by Red Mountain Formation.||
17932|Telemon Formation|69952|6|Mentioned|p1, p2 Tb.i, p120|Early Carboniferous|Early Carboniferous|Drummond Basin, overlying Thomson Orogen basement.||||||
17932|Telemon Formation|70856|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||Overlain conformably by Mount Hall Formation, unconformably overlies Silver Hills Volcanics.|Lithic sandstone and conglomerate, siltstone, algal limestone and minor tuffaceous siltstone.|
17932|Telemon Formation|70857|5|Briefly described|Map Legend|Carboniferous|Devonian|||||Overlain by Mount Hall Formation, overlies Foyle Volcanics|Lithic sandstone and conglomerate, siltstone, algal limestone and minor tuffaceous siltstone.|
17932|Telemon Formation|71710|6|Mentioned|p370 Fig 3|Early Carboniferous|Early Carboniferous|Geological province: southern Drummond Basin.||||Overlain by Mount Hall Formation. Underlain by Silver Hills Volcanics. Equivalent to Scartwater Formation in the northern Drummond Basin.||
17932|Telemon Formation|73198|4|Described|p499-500, p502-504, p507, p509-514|||Drummond Basin, south. Part of Cycle 2 of Olgers (1972). Basal unit of Cycle 2; disconformably overlies rocks of Cycle 1. Maximum thickness: 2100 m. Distinct enrichment of quartz and detrital muscovite mark change from the underlying Cycle 1 rocks. Northerly to north-easterly directed paleocurrent indicators. Basement provenance. [See article for petrographic descriptions and data].||||Underlain by Silver Hills Volcanics. Conformably overlain by Mount Hall Formation. Equivalent to Scartwater Formation.|Dominated by locally variable cross-bedded and sometimes ripple cross-laminated or horizontally bedded sandstones, siltstones and minor conglomerates.|
17948|Tenavute Microgranite|23291|5|Briefly described|p97 Tb. 3.11|Carboniferous|Carboniferous|Of the Newcastle Range I-types. Geological Province: Georgetown Region.||||||28-MAY-15
17948|Tenavute Microgranite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 27. Assumed to be I-Type.||||||
17948|Tenavute Microgranite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17948|Tenavute Microgranite|43259|4|Described|Appendix 1,p17.||Carboniferous|||||||
17948|Tenavute Microgranite|43740|4|Described|p16|||||||||
17948|Tenavute Microgranite|50198|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
17948|Tenavute Microgranite|50199|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
17948|Tenavute Microgranite|68353|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to brown, abundantly porphyritic microgranite, locally containing sparse chlorite.|
17948|Tenavute Microgranite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.|||||Grey to brown abundantly porphyritic microgranite, locally containing sparse chlorite.|
17948|Tenavute Microgranite|69593|5|Briefly described|p490|Permian|Carboniferous|Kidston Subprovince, Kennedy Igneous Association. Unassigned, but associated with the Newcastle Range Volcanic Group.|||||I-type: biotite microgranite and granite.|
17956|Tenningering Granodiorite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
17956|Tenningering Granodiorite|41778|2|Defined|Table 1|Permian||Described p370.||||||30-SEP-08
17956|Tenningering Granodiorite|43008|5|Briefly described|map legend|||||||||
17956|Tenningering Granodiorite|63821|5|Briefly described|p28|Late Permian|Early Permian|Age: 256+/-4Ma (K-Ar muscovite). Intrudes Curtis Island Group. Intruded by Wonbah Granodiorite and in contact with Wolca Granite. Comprises leucocratic, equigranular biotite granite, biotite granodiroite and muscovite-biotite granite.||||||07-FEB-11
17956|Tenningering Granodiorite|64556|5|Briefly described|p43-48, p56|Late Permian|Late Permian|Age of crystallisation: 259.0+/-2.0Ma (weighted mean). Age analysis details included. Sample analysed is from massive equigranular leucocratic biotite granodiorite.||||||07-FEB-11
17956|Tenningering Granodiorite|65452|5|Briefly described|p7 Tb.2|Guadalupian|Lopingian|SHRIMP U-Pb zircon magmatic crystallisation age.|259 +/- 2 Ma (Carson et al. 2006).||||Biotite-muscovite leuco-granodiorite.|
17956|Tenningering Granodiorite|68679|5|Briefly described|p421-422|||Gayndah-Gladstone belt.|259 +/- 2 Ma (SHRIMP: Carson et al., 2006).|||Adjacent to Wolca Granite.|Variable composition and texture. Biotite granodiorite, muscovite-biotite granodiorite; foliation; muscovite, garnet and altered cordierite suggests S-type.|
17956|Tenningering Granodiorite|71592|5|Briefly described|Appendix A.|||New England Orogen.|259+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
17956|Tenningering Granodiorite|73197|6|Mentioned|p476 Fig.7, p479|Guadalupian|Guadalupian|New England Orogen, northern, Hunter-Bowen Orogenic phase. S-type intrusive.|~270-260 Ma||||intrusives.|
17975|Termite Range Formation|22453|6|Mentioned|p 12|||||||||
17975|Termite Range Formation|22665|5|Briefly described|Table1 P222, P227||Statherian|Age of unit is 1605+/-5 Ma and 1636+/-10 Ma.  Actually written as Termite Range Fmn.||||||11-DEC-06
17975|Termite Range Formation|22680|6|Mentioned|84|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23031|6|Mentioned|40|||Geological province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Lawn Hill Formation; underlain by Riversleigh Siltstone.||||||11-DEC-06
17975|Termite Range Formation|23072|5|Briefly described|p754|||||||||
17975|Termite Range Formation|23363|5|Briefly described|351 Tab.1|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
17975|Termite Range Formation|23393|4|Described|p19, p21|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Age: 1636+/-10Ma, 1630+/-5Ma (Page & Sweet, 1998). Overlies the Riversleigh Siltstone; underlies the Lawn Hill Formation.||||||07-NOV-08
17975|Termite Range Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23397|5|Briefly described|p473|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23398|4|Described|p452|Statherian|Statherian|Of McNamara Group.||||||
17975|Termite Range Formation|23405|4|Described|p566|Statherian|Statherian|Of McNamara Group. 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23408|5|Briefly described|p513 Fig.2|||Of the McNamara Group.||||||11-DEC-06
17975|Termite Range Formation|23409|4|Described|p535 Fig.2|Statherian|Statherian|Age: 1636+/-10Ma.||||||11-DEC-06
17975|Termite Range Formation|23448|5|Briefly described|p479|||||||||
17975|Termite Range Formation|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
17975|Termite Range Formation|23958|3|Fully described|p1139|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 1300m.||||||07-NOV-08
17975|Termite Range Formation|23964|5|Briefly described|p1268|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 1100m. See also p1269 Table 1.||||||
17975|Termite Range Formation|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.   Geological Province:  Mount Isa Superbasin.||||||07-NOV-08
17975|Termite Range Formation|24309|5|Briefly described|p1013|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17975|Termite Range Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Riversleigh Siltstone. Overlain by Lawn Hill Formation. Age: 1636-1630 Ma. Geological Province: Lawn Hill Platform.||||||11-DEC-06
17975|Termite Range Formation|37459|2|Defined|p432|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
17975|Termite Range Formation|38237|4|Described|p130|||||||||
17975|Termite Range Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17975|Termite Range Formation|38310|6|Mentioned|p237|||||||||
17975|Termite Range Formation|38348|4|Described|p19|||||||||
17975|Termite Range Formation|38584|6|Mentioned|p22|||||||||
17975|Termite Range Formation|39497|6|Mentioned|p14|||See also Fig.4||||||
17975|Termite Range Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
17975|Termite Range Formation|39925|6|Mentioned|Fig.9|||||||||
17975|Termite Range Formation|43652|6|Mentioned|Fig.15,p393|||||||||
17975|Termite Range Formation|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
17975|Termite Range Formation|45166|5|Briefly described|p30|||||||||
17975|Termite Range Formation|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: 1636-1630 Ma. Conformably overlies Riversleigh Siltstone, conformably overlain by Lawn Hill Formation. Geological Province: Western Fold Belt.||||||19-DEC-07
17975|Termite Range Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Lithic and clayey sandstone, massive greywacke interbedded with shale and siltstone;  dark grey flaggy siltstone.||||||
17975|Termite Range Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Lawn Hill Formation, underlain by Riversleigh Siltstone.||||||
17975|Termite Range Formation|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||
17975|Termite Range Formation|62084|5|Briefly described|p936 Fig.5, p946 Fig.11, p948 Fig.13|Proterozoic|Proterozoic|Isa Superbasin. Lawn Hill. Shown as Termite Range Fm.||McNamara Group|||Variably dolomitic organic siltstones and shales.|
17975|Termite Range Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin. Consists of sandstone and conglomerate.||||||30-SEP-08
17975|Termite Range Formation|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Age: 1630+/-5 and 1636+/-10Ma. Geological Province: Isa Superbasin. Basal pebbly sandstones and conglomerate overlain by interbedded feldspathic and lithic sandstones and mudstones.||||||07-FEB-11
17975|Termite Range Formation|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||Part of Term supersequence.|1630 Ma.|Of the McNamara Group||Overlies ?unconformably Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Term supersequence.||||
17975|Termite Range Formation|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
17975|Termite Range Formation|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed.||||||
17975|Termite Range Formation|64250|6|Mentioned|p11 Fig.3|Statherian|Statherian||1630 +/- 5 Ma|Unit in McNamara Group.||||13-MAY-14
17975|Termite Range Formation|64317|6|Mentioned|p588 Fig. 1|||Appears in Fig. 1 as the term 'Lawn Hill and Termite Range Formation' but there is no reference in text.  Associated with the Termite Range Fault and Lawn Hill impact structure.||||||18-SEP-08
17975|Termite Range Formation|64575|6|Mentioned|p656 Fig. 1, p665|Proterozoic|Proterozoic|||||||
17975|Termite Range Formation|65228|5|Briefly described|p35, Fig.04.|Statherian|Statherian|Part of Term Supersequence in southern Lawn Hill Platform. SHRIMP zircon ages.|1636 +/- 10 Ma and 1630 +/- 5 Ma.|||Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|65337|5|Briefly described|p30.|||Correlative with Plain Creek Formation.|1647 +/- 8 to 1630 +/- 5 Ma (Page et al. 2000).|||Overlies Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|65396|5|Briefly described|p82, p175, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Lawn Hill Platform.|1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Formation; overlain by Lawn Hill Formation.||04-APR-17
17975|Termite Range Formation|66843|6|Mentioned|p38 Fig.10|||||||||
17975|Termite Range Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot.|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Mount Isa Block Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Isa Superbasin.|1630 +/- 10 Ma (maximum depositional age).|McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse, poorly sorted sandstone and lithic greywacke interbedded with laminated siltstone|
17975|Termite Range Formation|68542|6|Mentioned|p6|||||Upper McNamara Group||Disconformably overlies Riversleigh Siltstone, overlain by Lawn Hill Formation||
17975|Termite Range Formation|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Upper McNamara Group.||Overlies Riversleigh Siltstone. Is overlain by Lawn Hill Formation.||
17975|Termite Range Formation|68732|6|Mentioned|p165 Fig.3|Statherian|Statherian|Of the Term Supersequence. Sedimentary depositional age.|1630 +/- 5, 1636 +/- 10 Ma|||||
17975|Termite Range Formation|69591|4|Described|p43 Fig.2.31, p47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Constitutes the Term Supersequence. Submarine fan deposits: a series of medium- to coarse-grained clastic turbidite packages.|1636 +/- 10 Ma (MDA: Page et al., 2000).|McNamara Group.||Grades upwards into Lawn Hill Formation.|White to light brown and grey, thick-bedded, fine- to coarse, poorly sorted sandstone and lithic greywacke interbedded with laminated siltstone.|
17975|Termite Range Formation|69673|6|Mentioned|p54|||||||Correlated with Plain Creek Formation||
17975|Termite Range Formation|70897|6|Mentioned|Fig.1.7.7|||||||||
17975|Termite Range Formation|71369|5|Briefly described|p28|||||McNamara Group.||Is overlain unconformably by Schultz Sandstone Member.||
17975|Termite Range Formation|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1630+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Greywacke, siltstone, sandstone.|
17975|Termite Range Formation|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
17975|Termite Range Formation|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Equivalent to the Term Supersequence.||||||
17975|Termite Range Formation|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of McNamara Group.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone|
17975|Termite Range Formation|72416|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Lawn Hill Formation.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone|
17975|Termite Range Formation|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||White to light brown and grey, thick bedded, fine to coarse-grained, poorly-sorted quartzose to lithic, occasionally ferruginous sandstone interbedded with laminated siltstone|
17975|Termite Range Formation|72423|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of McNamara Group.|||Thin to medium-bedded, light brown clayey siltstone and ferruginous, fine to medium-grained sandstone. Thick bedded, poorly sorted sandstone interbedded with siltstone.|18-MAR-20
17975|Termite Range Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Ages given as U-Pb zircon sedimentary depositional ages for lower and upper parts of the unit.|1636 +/- 10 Ma to 1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.||
17975|Termite Range Formation|72527|6|Mentioned|p 132.|Statherian|Statherian|Described as being correlative with Riversleigh Siltstone.|c. 1647-1630 Ma|||Correlative with Riversleigh Siltstone Formation, Plain Creek Formation.|Includes tuffaceous volcanic material.|
17975|Termite Range Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Shown as being located in the Queensland part of the McNamara Group. Located in the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional ages given.|1630+/-5 Ma (upper), 1636+/-10 Ma (lower)|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.|Includes dolomitic siltstone.|
17975|Termite Range Formation|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p18, p19, p26.|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin.  Identified in 2 wells in this study. Mineral composition boxplots reveal dominant quartz, muscovite, albite and microcline components.|1630 +/- 5 Ma|McNamara Group||Overlies Riversleigh Siltstone and underlies Lawn Hill Formation.|Includes dolomitic siltstone.|
17975|Termite Range Formation|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
17975|Termite Range Formation|73042|6|Mentioned|p4, p12-13|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional ages See Fig 1.2, p4 (?maximum depositional age).|1630 +/- 5 Ma, 1636 +/- 10 Ma|McNamara Group||Underlain by the Riversleigh Siltstone. Overlain by Lawn Hill Formation.||
17975|Termite Range Formation|73098|6|Mentioned|p4, p7, p39|||Lawn Hill Platform. Organic petrolography performed on one sample from the Amoco DDH 83-2 well. Laminated component is characterised by alternations of bitumen-lean and bitumen-rich layers. [See report for bitumen/maceral description]|||||Includes laminated and non-laminated dark brown to dark grey shale.|
17975|Termite Range Formation|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. Part of the Term Supersequence. Leaky aquitard. Potential tight gas/oil. Includes oil show and gas show.||McNamara Group||Underlain by Riversleigh Siltstone. Overlain by Lawn Hill Formation.||
17984|Teroolinand Coal Measures|42648|6|Mentioned|p42|||New name, not reserved.||||||
17999|Terrica beds|42559|4|Described|p9|||Stated to be informal name. Variation on Terrica Beds.||||||
17999|Terrica beds|43008|5|Briefly described|map legend|||||||||
17999|Terrica beds|43745|6|Mentioned|p16||Permian|||||||
17999|Terrica beds|60937|5|Briefly described|p425 Fig. 3, p437|Early Permian|Early Permian|Geological Province: Terrica Inlier (Texas Block). See also p426 and p434.||||||14-APR-08
17999|Terrica beds|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic arenite, mudstone, siltstone; rare vitric tuff and conglomerate; locally fossiliferous.||||||
17999|Terrica beds|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic arenite, mudstone, siltstone; rare vitric tuff and conglomerate; locally fossiliferous.||||||29-APR-13
17999|Terrica beds|63748|5|Briefly described|p16, p18, p68|Permian|Permian|Of Lucas (1959, 1960c).Unconformable on and faulted against Texas beds. Interbedded med. to thick-banded, poorly sorted lithic arenite, mudstone and siltstone, with some vitric tuff and conglomerate. Permian fossils contained. Detailed lithology provided.||||||02-MAY-13
17999|Terrica beds|65107|6|Mentioned|p287|Sakmarian|Asselian|Permian inlier in the Texas beds.||||||
17999|Terrica beds|67908|6|Mentioned|p283|Permian.|Permian.|Texas Orocline. Early Permian.|||||Interbedded conglomerate, arenite, mudstone and siltstone layers.|
17999|Terrica beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Bondonga, Pikedale and Silver Spur beds, are all mapped under the symbol, Par.||||||
17999|Terrica beds|68679|5|Briefly described|p452, p455|Permian|Permian|Lucas (1959, 1960); Olgers and Flood (1970). Silver Spur Subprovince, Woolomin Province. 45km WNW of Stanthorpe. Coarser material derived from Texas beds. Contains a fauna similar to, but slightly younger than, Alum Rock Conglomerate.|||||Interbedded, medium- to thick-bedded, poorly sorted lithic sandstone, mudstone and siltstone with rare vitric tuff and conglomerate; sandstone is locally pebbly. Finer-grained material contains abundant plant material.|
17999|Terrica beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||27-SEP-18
17999|Terrica beds|70373|4|Described|p789-p792,  p795, p797 Tb 1, p798-p804|Early Permian|Early Permian|Fossils correlated with those in Alum Rock beds, suggesting Cisuralian age. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. Contain clasts of chert, sandstone, volcanic rocks thought to be derived from Texas beds. Other date from this unit: 297.8+/-4.3Ma. All LA-ICP-MS on zircon.  280-320m thick.|283.1+/-5.2 Ma, (LA-ICP-MS on zircons)|||Unconformably overlies and/or faulted against Texas beds. Correlated with Bondonga, Silver Spur, Pikedale and Alum Rock beds.|Sandstone, pebbly sandstone, conglomerate, diamictite and mudstone with clasts of chert, sandstone and volcanics. Crinoids and small spiriferid impressions present.|28-SEP-16
17999|Terrica beds|73487|6|Mentioned|p563, p574 Fig.8, p586|Sakmarian|Sakmarian|Upper Sakmarian in age (Archbold, 2001).||||||
18003|Teviot Formation|31621|6|Mentioned|p151|||||||||
18003|Teviot Formation|43987|14|Not recorded|p270,271,278|||||||||
18003|Teviot Formation|43994|14|Not recorded|Map Legend|||||||||
18003|Teviot Formation|43998|4|Described|p17,map||Triassic|||||||
18003|Teviot Formation|44000|14|Not recorded|p22,42,43,|||Overlies Carbrough Sandstone.||||||
18003|Teviot Formation|44001|14|Not recorded|Map Legend||Triassic|||||||
18003|Teviot Formation|44009|14|Not recorded|p68|||||||||
18003|Teviot Formation|48841|2|Defined|p1,31-34,46,48,Tb.I||Triassic|Conformably overlies Carborough Sandstone.||||||
18003|Teviot Formation|48915|6|Mentioned|Table 1|||Triassic||||||
18012|Texas beds|22601|6|Mentioned|405|Carboniferous|Carboniferous|||||||
18012|Texas beds|22857|5|Briefly described|p220, p502 App.1 Tb.A1.7|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
18012|Texas beds|22859|5|Briefly described|p220|||||||||
18012|Texas beds|23050|4|Described|p14 Table 1|Visean|Visean|Age: Early Carboniferous (Visean) age indicated by fossils.||||||
18012|Texas beds|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
18012|Texas beds|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Low grade regionally metamorphosed, variably deformed lithic wacke, conglomerate, siltstone, mudstone, chert, basalt and rare tuff.||||||20-DEC-04
18012|Texas beds|23812|5|Briefly described|p15|Early Carboniferous|Early Carboniferous|Intruded by Mole Granite.||||||
18012|Texas beds|24480|5|Briefly described|p6|Carboniferous|Carboniferous|||||||
18012|Texas beds|35020|6|Mentioned|p345|Early Carboniferous|Early Carboniferous|||||||
18012|Texas beds|36961|6|Mentioned|p216|||||||||
18012|Texas beds|38222|6|Mentioned|Fig.2|||||||||
18012|Texas beds|39071|6|Mentioned|p339|||||||||
18012|Texas beds|39413|6|Mentioned|p55|||||||||
18012|Texas beds|39943|6|Mentioned|Table 11A|||||||||
18012|Texas beds|39987|6|Mentioned|p65|||||||||
18012|Texas beds|40435|5|Briefly described|p47|||||||||
18012|Texas beds|40514|5|Briefly described|p3|||||||||
18012|Texas beds|40623|5|Briefly described|p107|||||||||
18012|Texas beds|40787|6|Mentioned|p346|||||||||
18012|Texas beds|40960|6|Mentioned|p216|||||||||
18012|Texas beds|42297|5|Briefly described|p3|Carboniferous||||||||
18012|Texas beds|42554|5|Briefly described|p47|||||||||
18012|Texas beds|42559|4|Described|p7|||||||||
18012|Texas beds|42729|5|Briefly described|p12|||||||||
18012|Texas beds|42748|6|Mentioned|Fig.3 P9|Carboniferous||||||||
18012|Texas beds|42901|5|Briefly described|Fig.12 P412|||||||||
18012|Texas beds|43008|5|Briefly described|map legend|||||||||
18012|Texas beds|43009|5|Briefly described|Map Legend|||||||||
18012|Texas beds|43582|6|Mentioned|p4|||||||||
18012|Texas beds|43745|6|Mentioned|Fig.4,p13|||||||||
18012|Texas beds|60079|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Hillgrove Suite.||||||
18012|Texas beds|60937|6|Mentioned|p422, p437|||Folded into a large synclinal structure.||||||02-MAY-13
18012|Texas beds|60993|5|Briefly described|p17|Paleozoic|Paleozoic|Unconformably overlain by Marburg Subgroup units.||||||07-NOV-08
18012|Texas beds|61392|5|Briefly described|p164 Fig. 1|Early Carboniferous|Late Devonian|||||||07-FEB-11
18012|Texas beds|61763|5|Briefly described|p25|Visean|Visean|A volcanic/limestone association. In the Texas Stanthorpe area. Geological Province: New England Orogen.||||||
18012|Texas beds|61770|6|Mentioned|p108|||||||||
18012|Texas beds|61796|5|Briefly described|p386 Fig. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||24-JAN-06
18012|Texas beds|62534|5|Briefly described|p6, p11 (legend)|Early Carboniferous|Early Carboniferous|Intruded by dykes of the "Willowrie diorite".||||||07-FEB-11
18012|Texas beds|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||04-JUN-07
18012|Texas beds|63729|5|Briefly described|Map legend|Carboniferous|Carboniferous|Volcaniclastic arenite, siltst., mudst., local phyllite, lenses of jasper, chert, limest.  Thin jasper interlayered with argillite, locally grading into chert. Recrystallised limest., local lst/basalt breccia. maif lava, minor chert. Polymictic pebble to||||||
18012|Texas beds|63731|5|Briefly described|Map legend|Carboniferous|Carboniferous|Volcaniclastic arenite, siltst., mudst.+slate; local phyllite. Altered chert, mafic volcs.+ volcaniclastic+slate sequences; massive greywacke; arenite+argillite; mafic lava; recrystallised limestone, local lst/basalt breccia; chert , argillite; jasper.||||||
18012|Texas beds|63732|5|Briefly described|Map legend|Carboniferous|Carboniferous|Arenite, siltst, mudst.,slate; local phyllite, lenses of jasper, chert, limstn.+mafic volcs. Altered chert, mafic volcs.+slate sequences. Recryst.chert+ interlayered mudst. Jasper+subordinate mudstone. Recrystallised limst.||||||02-MAY-13
18012|Texas beds|63733|5|Briefly described|Map legend|Carboniferous|Carboniferous|Arenite, siltst., mudst. and slate; lenses of jasper, chert, limestone+ mafic volcanics. Altered chert, mafic volcanics and slate sequences. Jasper with layered mudst. grading locally into chert. Recrystallised l'st., lst/basalt breccia. Mafic lava, ...||||||13-DEC-07
18012|Texas beds|63748|3|Fully described|p9-16|Early Carboniferous|Early Carboniferous|Unconformably overlain by Bondonga, Pikedale and Terrica beds. Intruded by Stanthorpe Granite, Greymare Granodiorite, Herries Granite. Geol.prov: Woolomin Province. Seq.of volcaniclastic turbidites (lithic arenite+mudstone). Detailed lithology provided.||||||07-FEB-11
18012|Texas beds|65107|5|Briefly described|p287|Carboniferous|Carboniferous|Contains inliers of Alum Rock Conglomerate and Terrica beds. Also infolded with Silver Spur inlier.||||||
18012|Texas beds|67669|6|Mentioned|p14,18|||Geological province: New England Fold Belt.||||||
18012|Texas beds|67908|5|Briefly described|p279-285|Carboniferous|Devonian|Olgers et al. (1974). New England Orogen. Bedding is steeply-dipping to sub-vertical. Primary structures examined; photographs.|||||A sequence of volcaniclastic turbidites with minor chert and jasper, altered mafic volcanic rocks and limestone. Shows slaty cleavage.|
18012|Texas beds|68003|5|Briefly described|p31, p140.|Early Carboniferous|Early Carboniferous|Central Block, New England Fold Belt. Coeval with Whitlow Formation.|||Includes Ashford Limestone [Member].||Low grade regionally metamorphosed, variably deformed lithic wacke, conglomerate, siltstone, mudstone, chert, basalt, basic and andesitic volcanics, fossiliferous limestone, marble, magnetite-rich rock and rare tuff.|
18012|Texas beds|68005|4|Described|p18, p22, pp33-35, p70, p155, p170.|Carboniferous|Carboniferous|Anaiwan terrane, Central Block, New England Fold Belt. Texas-Sandon association: a thick sequence of deep marine deposition; locally highly deformed; uppermost part of subduction complex. Contact metamorphosed up to 2 km around Mole Granite intrusion. Written as Texas Beds on p70.|||Includes Ashford Limestone.|Overlies Whitlow Formation. Is intruded by Mole Granite.|Dominantly turbidites; typically thin-bedded, coarse lithic wacke or conglomerate horizons, siltstone, mudstone with subordinate chert, jasper and spilite.|
18012|Texas beds|68006|5|Briefly described|p25, p85 Figs.7-Aa,Ab, p114, p115.|Early Carboniferous|Late Devonian|Deposited in a deep marine setting; forms part of a subduction complex. Limestone outcrops near Ashford are thought to represent a seamount within Texas beds sandstone. Written as Texas Beds on pp114-115.||||Overlies Whitlow Formation.|Sandstones.|
18012|Texas beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Texas Subprovince.||||||
18012|Texas beds|68679|5|Briefly described|p321, p446-453, p455-457, p463|Visean|Visean|Olgers et al. (1974); subdivided by Fergusson and Flood (1984) and Donchak et al. (2007). Most extensive unit in the Texas Subprovince, Woolomin Province, northern New England Orogen. Forms an arcuate, convex-north fold closure ~75km across. Numerous photographs; REE plot. Structure, age and provenance detailed. RELATED UNITS (continued): Is intruded by Ruby Creek, Clare Hills, Herries, Sailor Jack, Bullaganang, Mount You You, Granites; Boxwell, Greymare Granodiorites.||||Is overlain unconformably by the Wallangarra Volcanics (Wandsworth Volcanic Group), Texas and Pikedale beds. Correlated with Neranleigh-Fernvale beds and Wandilla Formation. See COMMENTS for more.|A succession of volcaniclastic turbidites (lithic sandstone and mudstone) with minor chert, jasper, argillite, altered mafic volcanics (greenstone) mostly alkalic basalts, and limestone. Lithologies and local variations described in detail.|
18012|Texas beds|68901|5|Briefly described|p8 Fig. iii|Carboniferous|Carboniferous|Woolowin Province.[probably typo for Woolomin].||||||27-SEP-18
18012|Texas beds|69600|5|Briefly described|p656-657|||Texas region. Contains karst topography features including numerous caves which contain diverse Quaternary fossil vetebrate faunas (described).|||||Includes limestone lenses up to 400m wide and 1000m long.|
18012|Texas beds|70036|5|Briefly described|Map legend|||Central Block, New England Fold Belt. Included in a mapped unit of Silurian to Carboniferous strongly deformed, andesitic to rhyolitic metasedimentary rocks, lithic sandstone, argillite, chert and jasper.||||||
18012|Texas beds|70373|5|Briefly described|p789, p791, p793, p800|Carboniferous|Devonian salt|||||Unconformably overlain by and/or faulted against Silver Spur, Terrica and Alum Rock beds. Cut by rhyolitic dyke that also cuts Bondonga beds.|Chert, sandstone and volcanic rocks (rhyolite dyke).|28-SEP-16
18012|Texas beds|71628|5|Briefly described|p4:33, 35; p5:2-3, 5-6, 10; p10:5, 9-10|Carboniferous|Carboniferous|See also p12: 10, 13, 18; p15: 33, 41, 43, 45, 82, 85, 89-90, 97; p18-10; p19: 6, 22, 27, 33, 59, 63, 65, 67, 70-71, 110, 145, 150, 157, 166, 171. Hosts various mineralisations including the Warroo Cu-Au mine, numerous small Au deposits W of Palgrave Monzogranite, and Back Creek and Sundown tin deposits. RELATED UNITS (continued): Is also intruded by Palgrave and Linton Monzogranites; Jibbinbar, Mount Bullaganang, Dumboy-Gragin, Wandera Leucosyenogranites; Mole, Treverton, Ruby Creek Leucogranites; Stanthorpe Complex; Amiens and Elsmore Leucomonzogranites; Greymare Tonalite; Cheviot Hills Granite; Pike Creek Dolerite; Willowrie Diorite; Reedy Gabbro. Is faulted against Passchendaele Monzogranite.||||Is intruded by Boxwell, Dry Creek, Kings Plains Granodiorites; Graman, Sailor Jack, Severn River, Strathaven, Benalla, Balladean, Herries, Clare Hills, Fairleigh Monzogranites. See COMMENTS for more.|Includes volcaniclastic arenite, phyllitic mudstone chert layers, sporadic meta-basalt flow and tuff; locally melange.|
18012|Texas beds|72297|5|Briefly described|p721|||Associated with arsenopyrite, cassiterite and copper in quartz greisen and sheeted veins at Sundown and Jibbinbar, where it is hornfelsed by the Ruby Creek Granite.||||Is intruded by Ruby Creek Granite.||
18012|Texas beds|73487|6|Mentioned|p563, p574 Fig.8|||||||||
18088|Thorntonia Limestone|8187|5|Briefly described|Map legend|Cambrian|Cambrian|Overlies Black Stump Arkose; underlies Georgina Limestone.||||||21-JUN-04
18088|Thorntonia Limestone|9830|5|Briefly described|Map Legend|Cambrian|Cambrian|Dolomitic limestone, dolomite, chert nodules. Underlies O'Hara Shale, Roaring Siltstone. Overlies Mount Birnie Beds.||||||01-FEB-07
18088|Thorntonia Limestone|10116|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Micrite, silicified limestone, black shale, sandstone, siltstone, minor coquinite.||||||
18088|Thorntonia Limestone|12951|4|Described|p143, 146, 149, 154-155, 157|Middle Cambrian|Middle Cambrian|Georgina Basin. Dolomitic beds. Previously called lower Hay River Formation, lower Arthur Creek Formation [in various parts of the Basin?]. Electric logs and core correlations have allowed reduction of names for rocks of this age and lithology to just Thorntonia Limestone.||||Overlies Red Heart Dolostone disconformably. Unconformably overlain by Arthur Creek Formation.|Grey dolostone, minor dolopackstone and dolograinstones. Nodular evaporite and dissolution structures are common. Interbeds of dark carbonaceous mudstone. Locally siliciclastic sandstone, siltstone at base.|
18088|Thorntonia Limestone|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia||||||||
18088|Thorntonia Limestone|23031|6|Mentioned|17|||Geological  province: Georgina Basin.||||||11-DEC-06
18088|Thorntonia Limestone|23072|5|Briefly described|p754|||||||||
18088|Thorntonia Limestone|23393|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|23408|5|Briefly described|p513|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin. carbonates.||||||15-JUN-09
18088|Thorntonia Limestone|23448|4|Described|p480|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|24308|5|Briefly described|p995 Fig. 8|||||||||
18088|Thorntonia Limestone|24419|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Regionally extensive layer of rubbly black to white banded and convoluted chert and chert breccia (Ardmore Chert Member). Overlies Riversdale Formation; conformably underlies & interfingers with Beetle Creek Formation. Geological Province: Georgina Basin.||||||13-APR-05
18088|Thorntonia Limestone|24432|6|Mentioned|p565 Fig.4|||||||||
18088|Thorntonia Limestone|24442|5|Briefly described|p45|Middle Cambrian|Middle Cambrian|Comprises predominantly dolostone, with local basal terrigenous sediments and a medial interval bearing pyritic-carbonaceous black shale interbeds.  Geological Province: Georgina Basin.||||||11-DEC-06
18088|Thorntonia Limestone|26310|4|Described|p9, Table 1|Middle Cambrian|Middle Cambrian|Maximum thickness: 150 feet.  Limestone and dolomite.||||||
18088|Thorntonia Limestone|29940|6|Mentioned|p169|||||||||
18088|Thorntonia Limestone|30239|5|Briefly described|p1193|||||||||
18088|Thorntonia Limestone|30242|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|31396|6|Mentioned|Fig.3|||||||||
18088|Thorntonia Limestone|32576|5|Briefly described|p49|||||||||
18088|Thorntonia Limestone|32952|4|Described|p1188|||See also pp1189-1194,1204,1209. M.-U. Cambrian.||||||11-DEC-06
18088|Thorntonia Limestone|33111|4|Described|p43|||||||||
18088|Thorntonia Limestone|33113|6|Mentioned|Fig.1|||Mid.Camb.||||||
18088|Thorntonia Limestone|33387|6|Mentioned|p349|||||||||
18088|Thorntonia Limestone|33482|6|Mentioned|Fig.2|||Early Middle Cambrian. Phosphate in.||||||
18088|Thorntonia Limestone|34287|6|Mentioned|Fig.3|||||||||
18088|Thorntonia Limestone|34543|6|Mentioned|p98|||||||||
18088|Thorntonia Limestone|34847|6|Mentioned|Table 1|||Stratigraphy & hydrocarbon prospects||||||
18088|Thorntonia Limestone|34935|6|Mentioned|p274|||||||||
18088|Thorntonia Limestone|35001|6|Mentioned|Fig.45|||||||||
18088|Thorntonia Limestone|35032|6|Mentioned|p117|||||||||
18088|Thorntonia Limestone|35054|6|Mentioned|Table 23|||||||||
18088|Thorntonia Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|35139|4|Described|Table.2|||||||||
18088|Thorntonia Limestone|35538|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|35553|6|Mentioned|p176|||Appendix containing description of Agnostid localities.||||||
18088|Thorntonia Limestone|36234|3|Fully described|p167|||See also p162.||||||11-DEC-06
18088|Thorntonia Limestone|36243|6|Mentioned|Table 1A|||||||||
18088|Thorntonia Limestone|36448|5|Briefly described|p395|||||||||
18088|Thorntonia Limestone|36644|6|Mentioned|p213|||||||||
18088|Thorntonia Limestone|36645|5|Briefly described|p314|||Fig.3,2.||||||
18088|Thorntonia Limestone|36818|6|Mentioned|p203|||See also Plate 57.||||||
18088|Thorntonia Limestone|37572|4|Described|p157|||See also Figs.7 and 8 and p165.||||||11-DEC-06
18088|Thorntonia Limestone|37816|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|38209|5|Briefly described|p175|||||||||
18088|Thorntonia Limestone|38291|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|38348|6|Mentioned|p24|||||||||
18088|Thorntonia Limestone|38350|6|Mentioned|p22|||||||||
18088|Thorntonia Limestone|38442|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
18088|Thorntonia Limestone|38444|5|Briefly described|p105|||||||||
18088|Thorntonia Limestone|38446|6|Mentioned|Table 23|||||||||
18088|Thorntonia Limestone|38608|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|39029|5|Briefly described|Map legend|Cambrian|Cambrian|||||||25-AUG-04
18088|Thorntonia Limestone|39425|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||11-DEC-06
18088|Thorntonia Limestone|39496|6|Mentioned|p16|||||||||
18088|Thorntonia Limestone|39562|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Grey crystalline limestone.||||||15-JUN-06
18088|Thorntonia Limestone|39690|6|Mentioned|Table 1|||||||||
18088|Thorntonia Limestone|39797|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|39921|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|39943|6|Mentioned|Table 2A|||||||||
18088|Thorntonia Limestone|40004|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
18088|Thorntonia Limestone|40137|6|Mentioned|p188|||||||||
18088|Thorntonia Limestone|40221|4|Described|p20|||||||||
18088|Thorntonia Limestone|40386|6|Mentioned|p429|||||||||
18088|Thorntonia Limestone|40623|5|Briefly described|p96|||See also p112.||||||11-DEC-06
18088|Thorntonia Limestone|40686|5|Briefly described|p407|||||||||
18088|Thorntonia Limestone|40810|6|Mentioned|p5|||||||||
18088|Thorntonia Limestone|40852|6|Mentioned|p37|||||||||
18088|Thorntonia Limestone|40855|6|Mentioned|p329|||||||||
18088|Thorntonia Limestone|40857|5|Briefly described|Table 21.1|||||||||
18088|Thorntonia Limestone|40858|5|Briefly described|p132|||||||||
18088|Thorntonia Limestone|41129|6|Mentioned|p17|||See also Fig.8.||||||13-SEP-18
18088|Thorntonia Limestone|41240|4|Described|p111|||||||||
18088|Thorntonia Limestone|41306|6|Mentioned|p4|||||||||
18088|Thorntonia Limestone|41388|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|41639|6|Mentioned|p3|||||||||
18088|Thorntonia Limestone|42060|6|Mentioned|Fig.5 P140|||||||||
18088|Thorntonia Limestone|42070|6|Mentioned|p4|||||||||
18088|Thorntonia Limestone|42575|5|Briefly described|Fig.2 P335|||||||||
18088|Thorntonia Limestone|42956|5|Briefly described|p31 Fig.4|||||||||
18088|Thorntonia Limestone|43105|5|Briefly described|Fig.4,p9.|||||||||
18088|Thorntonia Limestone|43807|6|Mentioned|Fig.2,p347|||||||||
18088|Thorntonia Limestone|43883|14|Not recorded|p18 Fig.4-3|||See also Lexicon.||||||
18088|Thorntonia Limestone|44091|14|Not recorded|p16,Tb.1,p18||Middle Cambrian|||||||
18088|Thorntonia Limestone|44098|14|Not recorded|p98||Cambrian|||||||
18088|Thorntonia Limestone|44209|14|Not recorded|p140,145-146||Cambrian|||||||
18088|Thorntonia Limestone|44211|2|Defined|p96-98,101-109|||||||||
18088|Thorntonia Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44271|14|Not recorded|p41|||See also Lexicon. Overlies Camooweal Dolomite. (lower Middle Cambrian)||||||
18088|Thorntonia Limestone|44273|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44274|2|Defined|Tb.1,p6,9,10,12,map||Middle Cambrian|Overlies? Camooweal Dolomite at Ixion Creek.||||||01-FEB-07
18088|Thorntonia Limestone|44275|14|Not recorded|Map Legend|||||||||
18088|Thorntonia Limestone|44276|2|Defined|p20,22,Tb.2,map|||||||||
18088|Thorntonia Limestone|44277|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44281|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44285|14|Not recorded|p.7|||||||||
18088|Thorntonia Limestone|44290|14|Not recorded|p439||Middle Cambrian|||||||
18088|Thorntonia Limestone|44309|2|Defined|Tb.1,p7-9,map|||No fossils. Unconformably overlies Precambrian.||||||
18088|Thorntonia Limestone|44326|14|Not recorded|Map Legend||Middle Cambrian|||||||
18088|Thorntonia Limestone|44441|14|Not recorded|p.8||Middle Cambrian|Middle Cambrian. Lawn Hill sheet (E54-9).||||||
18088|Thorntonia Limestone|44757|6|Mentioned|p153,155|||||||||
18088|Thorntonia Limestone|44920|14|Not recorded|Map Legend, Sheet2,4||Middle Cambrian|||||||
18088|Thorntonia Limestone|44922|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies the Camooweal Dolomite.  Thin-bedded to massive dolomite and dolomitic limestone, Girvanella limestone.||||||01-JUL-04
18088|Thorntonia Limestone|44989|14|Not recorded|p.102,110,118-202|||On many pages.||||||
18088|Thorntonia Limestone|45052|3|Fully described|p92|||M.Camb.||||||
18088|Thorntonia Limestone|45055|6|Mentioned|p9|||See also p20,25,29,34.||||||13-SEP-18
18088|Thorntonia Limestone|45079|3|Fully described|p18|||||||||
18088|Thorntonia Limestone|45102|6|Mentioned|p43|||||||||
18088|Thorntonia Limestone|45130|6|Mentioned|Fig.2|||||||||
18088|Thorntonia Limestone|45166|5|Briefly described|Table 15|||||||||
18088|Thorntonia Limestone|46955|6|Mentioned|p159|||||||||
18088|Thorntonia Limestone|46959|6|Mentioned|Table 1|||||||||
18088|Thorntonia Limestone|47024|6|Mentioned|p1|||||||||
18088|Thorntonia Limestone|47044|6|Mentioned|p191|||||||||
18088|Thorntonia Limestone|47058|5|Briefly described|p119|||||||||
18088|Thorntonia Limestone|47083|5|Briefly described|p19||Cambrian|||||||
18088|Thorntonia Limestone|48906|14|Not recorded|Tb.1|||||||||
18088|Thorntonia Limestone|49027|6|Mentioned|p3|||||||||
18088|Thorntonia Limestone|50100|5|Briefly described|p22|Middle Cambrian|Middle Cambrian|Typically consists of silicified and commonly brecciated dolomite and chert; contains sparse fossils.  Disconformably overlies the Mount Birnie beds; disconformably overlain by Beetle Creek Formation and Roaring Siltstone.||||||
18088|Thorntonia Limestone|50550|6|Mentioned|p1146 Fig.9|||Geological Province: Western Fold Belt.||||||19-DEC-07
18088|Thorntonia Limestone|50600|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Overlies Border Waterhole Formation. Grey crystalline limestone and dolomite, some chert interbeds.||||||13-SEP-18
18088|Thorntonia Limestone|60122|3|Fully described|p15, p4-5, p11 Tb. 1|Middle Cambrian|Middle Cambrian|Limestone, dolostone; medial pyritic-carbonaceous black shale interbeds; basal terriginous sst, greywacke. mudstone. Disconformable on Red Heart Dolostone; disconformable below Arthur Cr Fm; nonconformable on Mount Tietkens Gr.Complex. Max. thick: 103m.||||||23-MAY-05
18088|Thorntonia Limestone|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 103m. Disconformably overlies Red Heart Dolostone. Limestone, dolostone, black shale interbeds.||||||01-FEB-07
18088|Thorntonia Limestone|60264|5|Briefly described|p575 Fig. 1|Middle Cambrian|Middle Cambrian|Disconformably overlain by Monastery Creek Formation.  Geological Province: Burke River Inlier (Georgina Basin).||||||02-AUG-04
18088|Thorntonia Limestone|60359|5|Briefly described|Map Legend|Cambrian|Cambrian|Chert.||||||
18088|Thorntonia Limestone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Contains fauna of Ordian age.||||||
18088|Thorntonia Limestone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.  Overlies the Red Heart Dolostone (Tarlton Range area); overlain by Arthur Creek Formation.||||||25-NOV-04
18088|Thorntonia Limestone|60675|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Underlies Arthur Creek Formation. Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.||||||
18088|Thorntonia Limestone|61022|5|Briefly described|p14, p15 Fig. 2|Middle Cambrian|Middle Cambrian|Unconformably overlain by the lower Arthur Creek Formation.  Geological Province: Georgina Basin. Named in Abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||01-FEB-07
18088|Thorntonia Limestone|61155|5|Briefly described|p4|Cambrian|Cambrian|In northwest Queensland.||||||
18088|Thorntonia Limestone|61250|5|Briefly described|p43|Middle Cambrian|Middle Cambrian|Contains petroleum systems. Geological Province: Georgina Basin.||||||
18088|Thorntonia Limestone|61404|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Narpa Group. Dolostone, limestone; medial pyritic-carbobaceous black shale interbeds; basal terrigenous sandstone. Geological Province: southern Georgina Basin.||||||
18088|Thorntonia Limestone|61904|5|Briefly described|p132 Fig. 2|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|62376|5|Briefly described|p53|Middle Cambrian|Early Cambrian|Geological Province: Georgina Basin.||||||09-FEB-10
18088|Thorntonia Limestone|62759|5|Briefly described|p1|||Geological Province: Georgina Basin. Contains extremely rich, oil-prone microbial source rocks.||||||05-FEB-08
18088|Thorntonia Limestone|62789|5|Briefly described|p128, p129 Fig. 2, p132|Middle Cambrian|Middle Cambrian|In southern Georgina Basin. Fossiliferous. 58 m thick in Pacific Oil & Gas Baldwin No. 1 exploration well.||||Overlies Early Cambrian Red Heart Dolostone and underlies Middle Cambrian Arthur Creek Formation.||28-MAR-12
18088|Thorntonia Limestone|62790|5|Briefly described|p207, p209, p210, Fig. 2|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Thickness of 58.1 m in the Pacific Oil & Gas Baldwin No. 1 well. ?Superseded Yelvertoft Beds.||||Overlies Errarra Formation and is overlain by Arthur Creek Formation.||28-MAR-12
18088|Thorntonia Limestone|62983|6|Mentioned|p11|||Geological Province: Georgina Basin.||||||
18088|Thorntonia Limestone|63062|6|Mentioned|p41|||Age equivalent of Jigaimara Formation. Geological Province: Georgina Basin.||||||07-FEB-11
18088|Thorntonia Limestone|63450|5|Briefly described|p76, p78 Fig. 5, p80|Middle Cambrian|Middle Cambrian|Unconformable over Monastery Creek Member (Beetle Creek Formation). Max.thickness: 100m. Geol. province: Georgina Basin, East Toko Synline and Burke River Structural Belt. Limestone, dolostone, black shale and minor sandstone and mudstone. See also p81.||||||07-FEB-11
18088|Thorntonia Limestone|64068|3|Fully described|p57-59, p82-87, p61, 44, 53, 54|Middle Cambrian|Middle Cambrian|Widespread. Potential hydrocarbon source and reservoir rock. Potential host for epigenetic, stratiform, sediment-hosted Pb-Zn. Has been recognised in southern Georgina Basin outcrop and drillholes in which it was formerly assigned variously to the Arthur Creek Formation, lower Hay River Formation or upper Hay River Formation Member 1. Detailed petrography is provided. Diverse Ordian fauna including trilobites Redlichia and Xystridura.||Of Narpa Group.|Includes chertified dolostone of Yelvertoft Bed and 'Ardmore Chert Member', and dolomitic-phosphatic Bronco Stromatolith Bed, all at top.|Disconformably overlies Andagera Formation.|Grey limestone, dolostone, pyritic-carbonaceous dolostone, marl and mudstone; minor nodular chert, phosphorite.|22-FEB-16
18088|Thorntonia Limestone|64317|5|Briefly described|p587, p588-589, p597|Middle Cambrian|Middle Cambrian|Annular outcrop with ~18km diameter - the Lawn Hill impact structure coincides with its outer margin.  Age is Ordian: 520-510Ma. Thickness: <100m, but within annulus may be up to 400m? Geol. prov: Georgina Basin. Mainly dolostone and dolomitic limestone.||||||13-SEP-18
18088|Thorntonia Limestone|64443|5|Briefly described|iii, p5-9, p6 Tb.1, p40|Ordian|Ordian-Early Templetonian|In Undilla Sub-basin. Max 121m thick. Shows pervasive recrystallisation, nodular evaporite, hydrocarbons.||Of Narpa Group.||Unconformably overlies undivided South Nicholson Group. Disconformably underlies Wonarah Formation.|Dolosparstone; minor bioclast and oncoid dolosparstone and intraclast dolowackestone to dolograinstone; basal dolomitic quartz sandstone and conglomerate sourced from Mittiebah Sandstone.|13-SEP-18
18088|Thorntonia Limestone|64575|6|Mentioned|p656 Fig. 1|Cambrian|Cambrian|||||||
18088|Thorntonia Limestone|64676|6|Mentioned|p23, p25|Middle Cambrian|Middle Cambrian|Georgina Basin.||||||
18088|Thorntonia Limestone|64778|6|Mentioned|p13, 25-26|Cambrian|Cambrian|Southern Georgina Basin. Potential hydrocarbon source.||||||
18088|Thorntonia Limestone|64812|4|Described|p236, p241-4 (figures),  p246, p251|Middle Cambrian|Middle Cambrian|Unconformably overlain by Arthur Creek Formation. Geol.Prov: Georgina Basin. Basin-wide, upward shallowing platformal, dolomitised limestone sequence; contains organic-rich shales which are prospective, noted as "hot shale" (Fig. 2). Max. thickness: 900m.||||||07-FEB-11
18088|Thorntonia Limestone|64813|5|Briefly described|p254, p255, p256 Fig. 2|Middle Cambrian|Middle Cambrian|Basal sst, siltst.or quartzitic dolostone,followed by interbedded carbonaceous mudstone; then erosional activity+deepening marine conditions resulted in anoxic, pyritic + carbonaceous, partly dolomitic shale = basal 'hot shale' of Arthur Creek Fm. above.||||||13-SEP-18
18088|Thorntonia Limestone|65237|4|Described|p3 Fig. 4, p6|Middle Cambrian|Middle Cambrian|Max. thickness: 100m. Geological province: southern Georgina Basin. Sheet-like, dolomitised limestone, with subordinate black shale; top of unit is a regional unconformity marked by karstification. Further lith. detail included.||||||07-FEB-11
18088|Thorntonia Limestone|65239|5|Briefly described|p2|Middle Cambrian|Middle Cambrian|Unconformably underlies Arthur Creek Formation. Geological province: Georgina Basin.||||||
18088|Thorntonia Limestone|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Narpa Group. Unconformably overlies Helen Springs Volcanics of Kalkarindji Volcanic Group; unconformably underlies Wonorah Formation of Barkly Group. Dolostone, limestone; medial pyritic-carbonaceous black shale interbeds; basal terrigenous sandstone.||||||
18088|Thorntonia Limestone|65337|6|Mentioned|p65.|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, central and eastern Georgina Basin.||Unit in Narpa Group.||Unconformably overlies Kalkarindji Volcanic Group.||
18088|Thorntonia Limestone|65344|5|Briefly described|p3 Fig. 2 , p13, 24|||See thin section description for detail.||||Overlies South Nicholson Group. Overlain by Wonarah Formation.||
18088|Thorntonia Limestone|65345|5|Briefly described|pp1-2, p6 Fig.5, p8. |Cambrian|Cambrian|Georgina Basin. Positive tests in 1965-1966 for phosphate identified this unit as a target.||||Is unconformably overlain by Wonarah and Arthur Creek Formations.||
18088|Thorntonia Limestone|65489|5|Briefly described|p124-125, p127|Middle Cambrian|Middle Cambrian|Georgina Basin. Reservoir unit. Hosts the Lake Nash 1 tar and minor oil and gas show.||||Unconformably overlies Sylvester Sandstone. Is overlain by Monastery Creek Member (of Beetle Creek Formation).|Platform carbonates (dolomite).|
18088|Thorntonia Limestone|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.|||Marine bioclastic carbonate rocks.|
18088|Thorntonia Limestone|67323|5|Briefly described|GIS attrib tbl, p72, p83, p92 Fig.12.2|Middle Cambrian|Middle Cambrian|See also Solid Geology Map. Georgina Basin. Contains Pb, Zn and Pb-Zn anomalies 50-75km NE of Camooweal.||Narpa Group.||Overlies Sylvester Sandstone and (unconformably) Mount Birnie beds and Colless Volcanics. Is overlain by Beetle Creek Formation and (unconformably) by Georgina Limestone.|Grey crystalline limestone.|
18088|Thorntonia Limestone|67402|4|Described|p25 tbl RRM3|Templetonian|Ordian|Georgina Basin, East Toko Syncline. Maximum thickness of 100m. Deposited in a restricted marine environment. See also p213 fig GRG3, p214, p215, p217.||||Overlain by the Marqua beds, Arrinthrunga Formation, Inca Formation or Georgina Limestone. Unconformably overlies the Red Heart Dolomite.|Limestone, dolostone, black shale and minor sandstone and mudstone.|
18088|Thorntonia Limestone|67870|5|Briefly described|p38-39, p43-48, p50-54|Middle Cambrian|Early Cambrian|Georgina Basin. Identified as a pair of strong continuous seismic reflections. Potential hydrocarbon source rocks: 2% TOC, and reservoir. Detailed modelling showing transformation ratios, expulsion mass (bulk) and expulsions mass for oil and gas.||Narpa Group.||Unconformably overlies Mount Birnie beds. Is overlain unconformably by Beetle Creek Formation or Inca Shale.|Sandstone, organic-rich (3% TOC) shale; sections of chert.|
18088|Thorntonia Limestone|68020|6|Mentioned|p126|Cambrian|Cambrian|Includes phosphorite deposits.||||||
18088|Thorntonia Limestone|69206|6|Mentioned|p2|||Georgina Basin.||||||
18088|Thorntonia Limestone|69297|6|Mentioned|p288|Middle Cambrian|Early Cambrian|Age equivalent of the Jigaimara Formation.||||||
18088|Thorntonia Limestone|69377|5|Briefly described|map legend|Cambrian|Cambrian|||Narpa Group|||Thick-bedded dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|69418|5|Briefly described|p3:36|Middle Cambrian|Middle Cambrian|Georgina Basin. Contains potentially prolific marine source rocks.||||||12-JUL-16
18088|Thorntonia Limestone|69437|5|Briefly described|p22:9-10, 15-16|Series 2|Series 2|Western Undilla Sub-basin, and southern Georgina Basin, Centralian B Superbasin. Sequence 1. Peritidal to marine deposits. Potential petroleum source and reservoir rock.||||Overlies Helen Springs Volcanics. Is overlain by Wonarah, Arthur Creek Formations. Correlated with Border Waterhole Formation.|Limestone, dolostone, marl, phosphorite and some siliciclastic rocks.|12-JUL-16
18088|Thorntonia Limestone|69439|6|Mentioned|p24:10|||Georgina Basin.||||||12-JUL-16
18088|Thorntonia Limestone|69443|4|Described|p28:12,14,16-17,20-22, 1,38-40,43,45-47|Middle Cambrian|Middle Cambrian|Opik (1956). Widely distributed. The "Mount Hendry Formation" is said to be "probably basal Thorntonia Limestone". From 23 to >400m thick; usually <100m. Diverse fossil assemblage (listed). Peritidal to marine deposits, partly dysoxic to anoxic in the S and SW of the Basin. Exposed and karstified in Middle-Late Cambrian. Also overlies Riversdale Formation unconformably or gradationally. Is overlain by Beetle Creek Formation conformably to disconformably; by Arthur Creek, Inca, Gowers Formations and Bronco Stromatolith Bed disconformably; by Currant Bush Limestone and Barkly Group unconformably. Lateral equivalent of Border Waterhole Formation. Associated with minor Pb-Zn mineralisation in the Marqua-Boat Hill area, and hosts high-grade phosphorite in the Marqua and Ammaroo/Barrow Creek areas (Foss Hill and Ammaroo deposits). With basal Arthur Creek Formation, forms a reservoir-seal couplet. Has high hydrocarbon yields and is a potential source rock. Also a potential petroleum reservoir.||Basal Narpa Group.|Yelvertoft Bed, "Ardmore Chert Member".|Overlies Colless Volcanics and "Mount Hendry Formation" gradationally; Andagera Formation and Red Heart Dolostone disconformably; Shadow Group and Mount Birnie beds unconformably.|Mainly marine bioclastic carbonate rocks: limestone, partially dolomitised limestone, dolostone, pyritic-carbonaceous dolostone, marl and mudstone; minor nodular chert and phosphorite. Local thin basal quartz sandstone or arkosic conglomerate lag.|12-JUL-16
18088|Thorntonia Limestone|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Central and eastern Georgina Basin.||||Unconformably overlies Colless Volcanics (Kalkarindji Suite).||12-JUL-16
18088|Thorntonia Limestone|69446|6|Mentioned|p31:3|||Georgina Basin. Broadly age-equivalent to Daly River Group(Daly Basin).||||||12-JUL-16
18088|Thorntonia Limestone|69447|6|Mentioned|p32:2|||Georgina Basin.||||Age-equivalent to Montejinni Limestone, Hooker Creek Formation and Lothari Hill Sandstone (Wiso Basin).||12-JUL-16
18088|Thorntonia Limestone|69448|6|Mentioned|p33:3|||Georgina Basin.||||Correlated with Negri Subgroup (Ord Basin) in part.||12-JUL-16
18088|Thorntonia Limestone|69561|5|Briefly described|p33 fig 2, p34|Ordian|Ordian|Ordian age confirmed by trilobite fossil assemblage in siltstone of overlying Arthur Creek Formation.||||Overlies Helen Springs Volcanics, Overlain by Wonarah Formation, Arthur Creek Formation|Limestone.|
18088|Thorntonia Limestone|69591|4|Described|p87-91, p94, p96-97|Cambrian|Neoproterozoic|Georgina Basin. Rarely >20m thick, but may be up to 100m thick. RELATED UNITS (continued): Is overlain by Inca Formation conformably, by Currant Bush Limestone, Blazan Shale or Age Creek Formation disconformably, and by Gowers Formation paraconformably.||Narpa Group.|Bronco Stromatolith.|Overlies Sylvester Sandstone (transitionally), Mount Birnie beds and (conformably) Riversdale Formation. Is overlain conformably by/locally grades into Beetle Creek Formation. See COMMENTS for more.|Includes thick-bedded dolomitic limestone, dolomite, phosphatic dolostone and bedded limestone with layers and nodules of chert. In places the limestone grades into shale, siltstone or fine sandstone. Richly fossiliferous.|
18088|Thorntonia Limestone|69673|4|Described|p116, p120,  p129,  p137, p138, p142,|Cambrian|Cambrian|23m - greater than 400m thick. Age derived from fossil assemblage.  Source rock with potential as a reservoir rock also.||Narpa Group||Disconformably overlain by Arthur Creek Formation|Limestone, dolomitised limestone, dolostone, pyritic carbonaceous dolostone, mudstone and marl with minor nodular chert and phosphorite.|07-MAR-23
18088|Thorntonia Limestone|70098|5|Briefly described|p7|||Georgina Basin. Approximate age equivalent of Jigaimara Formation.||||||
18088|Thorntonia Limestone|70303|5|Briefly described|iv, p15|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Nonconformably overlies the Mount Tietkens Granite Complex.||
18088|Thorntonia Limestone|70321|6|Mentioned|p154-155|Cambrian|Cambrian|Riversleigh region. Overlain, down-cut and/or framed by much younger (Cenozoic/Tertiary) freshwater limestones containing vertebrate fossils. Their geochemical analyses tabulated.|~500 Ma.||||An extensive marine dolostone (variably dolomitised limestone).|
18088|Thorntonia Limestone|70380|6|Mentioned|p745|Stage 5|Stage 4|Georgina Basin.||||||
18088|Thorntonia Limestone|70723|5|Briefly described|p21-29, p31|Cambrian|Cambrian|Georgina Basin. Defined at the Thorntonia Station in Qld; known informally as Hay River Formation. Organic-rich shales have ben targeted for hydrocarbons: oil- and gas-prone source rock. Deposited in peritidal to marine environments under dysoxic to anoxic conditions. Kerogen type and biomarker compositions discussed in detail. Series 2-3 age.||Narpa Group||Overlies Red Heart Dolostone. Overlain by Arthur Creek Formation, Blazan Shale or Beetle Creek Formation.|Vuggy, partially dolomitized limestone, pyritic-carbonaceous dolostone, marl and mudstone. Abundant phosphatic shell fragments and algal mats.|
18088|Thorntonia Limestone|70752|6|Mentioned|p129, p141|Middle Cambrian|Middle Cambrian|Georgina Basin. Ordian. Brachiopod systematic palaeontological descriptions.||||||
18088|Thorntonia Limestone|70951|5|Briefly described|p1069,1072,1074,1076-1077,1080-1084|||Geological province: Georgina Basin. Dolomite-dominated in both SWIR and TIR wavelengths.||Unit of Narpa Group.||Overlain by Arthur Creek Formation. Underlain by basement.||
18088|Thorntonia Limestone|71502|5|Briefly described|p1-2, p8|Cambrian|Cambrian|Generally weakly phosphatised, especially in shallower depositional zones. Some exposures are silcretised. Overlies Proterozoic units of the Lawn Hill Platform. [Also written as Precambrian in Fig.8].||||Unconformably overlain by Carl Creek Limestone.|Marine carbonates with interbedded cherty material. Contains phosphatised stromatolites, ovoid phosphate nodules and invertebrate fossils. Extensively dolomitised.|
18088|Thorntonia Limestone|71621|6|Mentioned|p25|Middle Cambrian|Middle Cambrian|Georgina Basin. Unconformably overlies unnamed orthogneiss reported to have an igneous crystallisation age of 1846 ± 6 Ma.||||||02-FEB-19
18088|Thorntonia Limestone|72297|5|Briefly described|p752|Cambrian|Cambrian|Georgina Basin.|||||Contains thin oil shale beds.|
18088|Thorntonia Limestone|72321|5|Briefly described|Fig 2, p3, 4, 7|Wulian|Wulian|Undilla Sub-basin, Georgina Basin. Type area in Undilla Sub-basin where age Cambrian Series 3, Stage 5. Redefined to exclude older rocks (now Hay River Formation), across southern portion of the basin. Australian Stage: Templetonian.||of Narpa Group.||Correlated with the lower Arthur Creek Formation in the Dulcie Syncline.||
18088|Thorntonia Limestone|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Narpa Group.||Overlain gradationally by Camooweal Dolomite. Underlain gradationally by Border Waterhole Formation.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|72415|4|Described|mapsheet|Early Ordovician|Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Narpa Group.||Overlain gradationally by Camooweal Dolomite. Underlain gradationally by Border Waterhole Formation.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert|
18088|Thorntonia Limestone|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites, brachiopods, molluscs.||Narpa Group||Disconformably overlain by the Arthur Creek Formation.|Limestone, dolomitised limestones, dolostone, pyritic-carbonaceous dolostone, marl, mudstone; minor nodular chert; phosphorate; local basal conglomerate, sandstone, greywacke.|
18088|Thorntonia Limestone|72516|3|Fully described|p12, p90-92|Cambrian|Cambrian|Georgina Basin. Occurs in HUCKITTA, ELKEDRA, SANDOVER RIVER, TOBERMORY, HAY RIVER, URANDANGI, DUCHESS, GLENORMISTON and JERVOIS RANGE SPECIAL map sheets. Contains fossil trilobites, archaeocipides, brachiopods and molluscs. Fossil assemblage indicates a Series 2 and Series 3 age of the Cambrian. Deposited in a peritidal to marine, partly dysoxic to anoxic environment. Thickness ranges from 23 to over 400m thick in the mapped area. Intersected in NTGS Huckitta 1 drillcore. Equivalent to the Gum Ridge Formation, Top Springs Limestone, Border Waterhole Formation and the Bronco Stromatolith Bed. Age equivalent of the Chandler Formation and the Giles Creek Dolostone of the Amadeus Basin.||Narpa Group||Disconformably overlain by the Arthur Creek Formation. Disconformably overlies the Red Heart Dolostone.|Limestone, dolomitised limestone, dolostone, pyritic-carbonaceous dolostone, marl, mudstone; minor nodular chert; phosphorate; local basal conglomerate, sandstone, greywacke.|02-JUN-21
18088|Thorntonia Limestone|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.||Narpa Group|||Thick-bedded , dolomitic limestone and dolomite with layers and nodules of chert.|
18088|Thorntonia Limestone|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).||Narpa Group||Underlies Roaring Siltstone and unconformably overlies the Shadow Group.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert and chert breccia.|
18088|Thorntonia Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
18088|Thorntonia Limestone|73288|5|Briefly described|p697-700, 702-703, 705, 707, 709 Fig.10|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Peritidal to marine platform setting. Non-economic oil and gas shows have been recorded. Downhole (Hylogger) logs; scratch test results tabulated. See also p710, 713.||Narpa Group.||Is overlain unconformably by Arthur Creek Formation.||07-MAR-23
18088|Thorntonia Limestone|73418|5|Briefly described|p3, p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin.||Narpa Group||Overlies Hay River Formation, underlies Beetle Creek Formation|Limestone, commonly phosphatic near the top.|
18102|Three Moon Conglomerate|22977|5|Briefly described|p67 Fig.2|Carboniferous|Carboniferous|||||||
18102|Three Moon Conglomerate|23037|5|Briefly described|p34||Early Carboniferous|Possible correlation with Torsdale beds. Yarrol Province.||||||05-NOV-07
18102|Three Moon Conglomerate|23468|4|Described|p 304|||also see Fig 2 p 295.||||||05-NOV-07
18102|Three Moon Conglomerate|24076|5|Briefly described|p397 Fig. 2|Early Carboniferous|Early Carboniferous|Max. thickness: 700m.  Geological Province: Yarrol Basin.||||||
18102|Three Moon Conglomerate|24399|5|Briefly described|p275, p272 Fig. 1|Late Devonian|Late Devonian|Volcaniclastic sediments, minor limestone and varying proportions of primary volcanic rocks.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt.||||||
18102|Three Moon Conglomerate|24467|5|Briefly described|p392 Fig.12|Early Carboniferous|Late Devonian|Ignimbrite - sourced sandstones. Geological Province: Yarrol Terrane||||||
18102|Three Moon Conglomerate|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
18102|Three Moon Conglomerate|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
18102|Three Moon Conglomerate|24491|4|Described|p18|Late Devonian|Late Devonian|Overlies Lochenbar beds and underlies Rockhampton Group in the Cania area.||||||
18102|Three Moon Conglomerate|24615|5|Briefly described|CD|Early Carboniferous|Late Devonian|[DCt].||||||
18102|Three Moon Conglomerate|30451|3|Fully described|p18|||See also p19,20. Early Carboniferous age.||||||18-AUG-08
18102|Three Moon Conglomerate|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous.||||||18-AUG-08
18102|Three Moon Conglomerate|31659|6|Mentioned|p47|||||||||
18102|Three Moon Conglomerate|31999|6|Mentioned|p149|||Table 1||||||
18102|Three Moon Conglomerate|32140|6|Mentioned|p149|||||||||
18102|Three Moon Conglomerate|32141|6|Mentioned|p149|||||||||
18102|Three Moon Conglomerate|32866|6|Mentioned|p7|||Fossil content.||||||18-AUG-08
18102|Three Moon Conglomerate|33728|6|Mentioned|p41|||||||||
18102|Three Moon Conglomerate|34085|6|Mentioned|Cor.chart|||Tournaisian||||||
18102|Three Moon Conglomerate|36235|6|Mentioned|Fig.1|||||||||
18102|Three Moon Conglomerate|36528|6|Mentioned|p171|||||||||
18102|Three Moon Conglomerate|36825|6|Mentioned|p5|||||||||
18102|Three Moon Conglomerate|37109|6|Mentioned|p283|||||||||
18102|Three Moon Conglomerate|38153|6|Mentioned|p366|||||||||
18102|Three Moon Conglomerate|38447|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
18102|Three Moon Conglomerate|39445|5|Briefly described|Table 6|||||||||
18102|Three Moon Conglomerate|41246|6|Mentioned|Map legend|Carboniferous||||||||
18102|Three Moon Conglomerate|42547|4|Described|p49|||||||||
18102|Three Moon Conglomerate|43461|14|Not recorded|Table p618||Tournaisian|||||||
18102|Three Moon Conglomerate|44360|14|Not recorded|p4,30,31,33||Tournaisian|(Late Tournaisian)||||||
18102|Three Moon Conglomerate|44379|2|Defined|p1-3,7-11,15,23-25,||Tournaisian|Tb.3, map. Correlated with Pond Argillites. (Early Tournaisian).||||||05-NOV-07
18102|Three Moon Conglomerate|45097|6|Mentioned|Fig.|||Correlation chart||||||
18102|Three Moon Conglomerate|46803|6|Mentioned|Fig. 4|||||||||
18102|Three Moon Conglomerate|50190|6|Mentioned|p21|||Hornfelsed andesitic volcanics contain mineralisation.||||||05-NOV-07
18102|Three Moon Conglomerate|50197|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|||||||
18102|Three Moon Conglomerate|50214|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Overlies Lochenbar Formation; underlies Rockhampton Group.||||||17-MAY-04
18102|Three Moon Conglomerate|50598|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Andesitic to basaltic polymitic conglomerate, sandstone, siltstone, mudstone, andesite, minor felsic tuff and limestone.||||||
18102|Three Moon Conglomerate|60282|5|Briefly described|p9|||Geological Province: Yarrol Province.||||||
18102|Three Moon Conglomerate|61392|5|Briefly described|p165 Fig. 2|Famennian|Frasnian|Part of the 'Bindawallah Stratigraphic Assemblage'.||||||07-FEB-11
18102|Three Moon Conglomerate|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Late Devonian|Includes the Monal Volcanic Facies Association of Bryan et al (2001). Fine-grained with widespread distribution of rip-up clast conglomerate, small amounts of quartz locally and limestone lenses are absent. Geol Prov: Yarrol Province. See also p1000 Fig.3||||||
18102|Three Moon Conglomerate|63600|5|Briefly described|p900 Fig. 1, p915|Early Carboniferous|Late Devonian|Part of the volcanic/sedimentary sequences unconformably overlying Capella Creek Group.||||||07-FEB-11
18102|Three Moon Conglomerate|64398|5|Briefly described|Map legend|Carboniferous|Late Devonian|Green-grey to purple, granule to cobble, andesitic to basaltic polymictic conglomerate, lithofeldspathic to feldspatholithic sandstone, siltstone, mudstone, andesite, minor felsic tuff, fossiliferous limestone; rare basaltic pillow lava and hyaloclastite.||||||18-AUG-08
18102|Three Moon Conglomerate|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Green grey to purple, granule to cobble, andesitic to basaltic polymictic conglomerate, lithofeldspathic to felspatholitic sandstone, siltstone, mudstone, andesite, minor felsic tuff, fossiliferous limestone; rare basaltic pillow lava and hyaloclastite.||||||
18102|Three Moon Conglomerate|65388|5|Briefly described|p19, 42, 69, 72, 158|Late Devonian|Late Devonian|Yarrol Provice. Correlated by Dear & others (1971), with Torsdale beds, but this correlation may not be valid. Includes basaltic volcaniclastics. Structurally interleaved with Lochenbar Formation (including basalts). May correlate with mafic facies of  Campwyn Volcanics.||||||
18102|Three Moon Conglomerate|68008|3|Fully described|p52, p61, p64-65, p67, p69, p71-80, p90|Late Devonian|Late Devonian|See also p92, p109, p132, p209, p213, p372, p375, p381, p400, p413, p488, p573, p581, p593, p603, p630, p635. Dear (1968). Subsequently included similar lithologies (recognised by Dear et al., 1971) in Unit A of the Crana beds (McKellar, 1967). The type section (described) is from GR294400 7279500 and GR297100 7274800 on the Scoria 100k sheet. ~750m to 1300m thick. Details of a representative section given. Is overlain by Rockhampton Group conformably, and by Youlambie Conglomerate, Winterbourne and Dooloo Tops Volcanics unconformably. Mature island-arc deposits: entirely marine. Lithologies described and illustrated in detail. Geochemistry discussed. Fauna, coral species, listed. Hosts the Maxwelton Goldfield. Micropaleontology table. Shelly fossils listed. Geophysics modelled.||||Is intruded by Bocoolima, Rocky Point, Monal Granodiorites, and Munholme Quartz Diorite. At least partly equivalent to Mount Alma, Mount Hoopbound and Lochenbar Formations. See Comments.|Fine- to coarse-grained purplish sandstone, poorly sorted conglomerate, grey to green siltstone, and minor basic to intermediate lavas including pillow basalt, and basaltic hyaloclastite.|
18102|Three Moon Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Early Carboniferous|Late Devonian|Yarrol Province. This unit, as well as the Mount Alma, Balaclava, Lochenbar and Mount Hoopbound Formations, the Tanderra Volcanics and the Channer Creek beds, are all mapped under the symbol, DCa.||||||
18102|Three Moon Conglomerate|68679|5|Briefly described|p310, p312-313, p337-339, p341, p344|Late Devonian|Late Devonian|See also p346, p425, p468. Dear (1968). Similar rocks mapped by McKellar (1967), as Unit A of the Crana beds, were added (Dear et al., 1971). Yarrol Province. The basalts are typical of mature island arcs and backarc basins.||||Is intruded by Bocoolima, Rocky Point Granodiorites.|Purple sandstone and poorly sorted conglomerate, greenish siltstone and minor basic to intermediate lavas including pillow basalt and hyaloclastite; interbedded fine-grained sandstone and siltstone.|
18119|Tiaro Coal Measures|22845|6|Mentioned|Fig6|Jurassic|Triassic|||||||
18119|Tiaro Coal Measures|22846|6|Mentioned|Plate 1|Jurassic|Late Triassic|||||||
18119|Tiaro Coal Measures|23251|5|Briefly described| Table 1 p6, p26||Early Jurassic|Age based on early Jurassic miospores. Geological Province: Maryborough Basin. Underlying unit Myrtle Creek Sandstone.||||||21-JUN-06
18119|Tiaro Coal Measures|23841|4|Described|p448|Jurassic|Jurassic|Geological Province: Maryborough Basin.  Maximum thickness: >1370m.||||||
18119|Tiaro Coal Measures|24382|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Parent: Duckinwilla Group||||||
18119|Tiaro Coal Measures|29651|6|Mentioned|Table 1|||||||||
18119|Tiaro Coal Measures|29960|6|Mentioned|p8|||Jurassic||||||
18119|Tiaro Coal Measures|30451|6|Mentioned|p77|||||||||
18119|Tiaro Coal Measures|30508|6|Mentioned|p91|||Palynological examination of cores||||||
18119|Tiaro Coal Measures|30654|4|Described|p47|||See also P49,50,53,55,56. Jurassic||||||
18119|Tiaro Coal Measures|30655|6|Mentioned|p20|||||||||
18119|Tiaro Coal Measures|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
18119|Tiaro Coal Measures|30916|6|Mentioned|p97|||||||||
18119|Tiaro Coal Measures|32137|4|Described|p35|||Lithology and palynology||||||
18119|Tiaro Coal Measures|32774|5|Briefly described|Table 2|||||||||
18119|Tiaro Coal Measures|34134|6|Mentioned|Cor.Chart|||Lower - Upper Jurassic||||||
18119|Tiaro Coal Measures|34287|6|Mentioned|p171|||Jurassic||||||
18119|Tiaro Coal Measures|34949|6|Mentioned|p155|||||||||
18119|Tiaro Coal Measures|35101|3|Fully described|p55|||||||||
18119|Tiaro Coal Measures|35813|6|Mentioned|p574|||||||||
18119|Tiaro Coal Measures|36101|6|Mentioned|p171|||||||||
18119|Tiaro Coal Measures|36243|6|Mentioned|Table 9A|||||||||
18119|Tiaro Coal Measures|36327|6|Mentioned|p7|||||||||
18119|Tiaro Coal Measures|36574|4|Described|p599|||Palynostratigraphy.||||||
18119|Tiaro Coal Measures|36575|4|Described|p596|||||||||
18119|Tiaro Coal Measures|36708|6|Mentioned|p52|||||||||
18119|Tiaro Coal Measures|36926|6|Mentioned|p162|||See also P165.||||||
18119|Tiaro Coal Measures|37065|6|Mentioned|p39|||||||||
18119|Tiaro Coal Measures|37118|4|Described|p317|||||||||
18119|Tiaro Coal Measures|37120|6|Mentioned|p321|||||||||
18119|Tiaro Coal Measures|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
18119|Tiaro Coal Measures|37463|6|Mentioned|p479|||||||||
18119|Tiaro Coal Measures|37618|4|Described|p22|||||||||
18119|Tiaro Coal Measures|37861|6|Mentioned|p591|||||||||
18119|Tiaro Coal Measures|38309|3|Fully described|p225|||||||||
18119|Tiaro Coal Measures|38397|4|Described|Table 2|||||||||
18119|Tiaro Coal Measures|38402|6|Mentioned|p72|||||||||
18119|Tiaro Coal Measures|39211|6|Mentioned|p41|||Freshwater.Jurassic.||||||
18119|Tiaro Coal Measures|39315|6|Mentioned|Fig.5|||||||||
18119|Tiaro Coal Measures|39445|5|Briefly described|Table 10|||||||||
18119|Tiaro Coal Measures|39505|6|Mentioned|p191|||||||||
18119|Tiaro Coal Measures|39943|6|Mentioned|Table 11A|||||||||
18119|Tiaro Coal Measures|40623|5|Briefly described|p54|||See also P104||||||
18119|Tiaro Coal Measures|41738|5|Briefly described|p173|||||||||
18119|Tiaro Coal Measures|41778|6|Mentioned|p376|||||||||
18119|Tiaro Coal Measures|41917|6|Mentioned|p522|||||||||
18119|Tiaro Coal Measures|42187|6|Mentioned|Fig.5 P322|||||||||
18119|Tiaro Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
18119|Tiaro Coal Measures|42282|6|Mentioned|p3|Jurassic||||||||
18119|Tiaro Coal Measures|42316|6|Mentioned|p8|||||||||
18119|Tiaro Coal Measures|42450|5|Briefly described|p407|||||||||
18119|Tiaro Coal Measures|42616|4|Described|p7|||||||||
18119|Tiaro Coal Measures|42636|6|Mentioned|p8|||||||||
18119|Tiaro Coal Measures|42648|5|Briefly described|Fig.7 P43|||||||||
18119|Tiaro Coal Measures|42695|5|Briefly described|Fig.2|Jurassic||||||||
18119|Tiaro Coal Measures|42751|5|Briefly described|p27|||see also Fig.1 P23||||||
18119|Tiaro Coal Measures|42893|5|Briefly described|p12|||||||||
18119|Tiaro Coal Measures|42894|2|Defined|p23|Middle Jurassic|Early Jurassic|see also Fig.2 P22||||||
18119|Tiaro Coal Measures|43008|5|Briefly described|map legend|||of Duckinwilla Group?||||||
18119|Tiaro Coal Measures|43059|6|Mentioned|p9|||of Duckinwilla Group||||||
18119|Tiaro Coal Measures|43100|4|Described|p45|Early Triassic||Of Duckinwilla Group.||||||14-AUG-08
18119|Tiaro Coal Measures|43252|6|Mentioned|p73|||||||||
18119|Tiaro Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||See also Lexicon.||||||
18119|Tiaro Coal Measures|43995|14|Not recorded|Tb.p10||Jurassic|||||||
18119|Tiaro Coal Measures|44029|14|Not recorded|p155,168|Late Jurassic|Early Jurassic|||||||
18119|Tiaro Coal Measures|44077|14|Not recorded|p298|||||||||
18119|Tiaro Coal Measures|44084|14|Not recorded|p32(Tb)|Late Jurassic|Early Jurassic|||||||
18119|Tiaro Coal Measures|44091|14|Not recorded|p58,63||Jurassic|||||||
18119|Tiaro Coal Measures|44240|14|Not recorded|p334|||||||||
18119|Tiaro Coal Measures|44241|2|Defined|p5,6,12,16,Fig.1,|Middle Jurassic|Early Jurassic|Map, Table 2. Tiaro Coal Measures form Myrtle Creek Series, formerly "Tiaro Series"||||||
18119|Tiaro Coal Measures|44385|14|Not recorded|p6|||||||||
18119|Tiaro Coal Measures|44387|14|Not recorded|p17|||||||||
18119|Tiaro Coal Measures|44616|14|Not recorded|p30,33||Jurassic|Tight.||||||
18119|Tiaro Coal Measures|44750|14|Not recorded|p12,16||Jurassic|||||||
18119|Tiaro Coal Measures|44752|2|Defined|p297-299|||Equivalent of Walloon Coal Measures. Unconformably overlain by Graham's Creek Formation.||||||
18119|Tiaro Coal Measures|44753|5|Briefly described|p47,49,5-54||Early Jurassic|Maryborough Basin.||||||
18119|Tiaro Coal Measures|44762|14|Not recorded|opp.p34||Jurassic|||||||
18119|Tiaro Coal Measures|44783|14|Not recorded|p2,39,41,42|||||||||
18119|Tiaro Coal Measures|44786|14|Not recorded|p193-202||Jurassic|||||||
18119|Tiaro Coal Measures|44923|5|Briefly described|Map Legend||Early Jurassic|||||||
18119|Tiaro Coal Measures|44928|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
18119|Tiaro Coal Measures|45440|14|Not recorded|p.7,14,15,25,29-88||Jurassic|Tb.1. On many pages. Of Walloon Series.||||||
18119|Tiaro Coal Measures|50320|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|||||||
18119|Tiaro Coal Measures|60077|5|Briefly described|Map legend|Middle Jurassic|Early Jurassic|Sandstone, siltstone, shale, coal, conglomerate, limestone, volcanics.||||||15-JUL-04
18119|Tiaro Coal Measures|60281|5|Briefly described|p36|Early Jurassic|Early Jurassic|Of Duckinwilla Gp. Consists of shale, mudstone, sltst., sst., coal, volcanics and some limestone. Conformably overlies Myrtle Ck.Sst; unconformably overlain by Graham Cr. Fm. in the Gundiah Embayment. Geol. Prov: Maryborough Basin.||||||22-MAR-05
18119|Tiaro Coal Measures|60998|5|Briefly described|p145|||Contains a ferruginous oolite marker unit about 400m above the base.||||||
18119|Tiaro Coal Measures|61611|6|Mentioned|p264, p267, p265 Fig. 3|Early Jurassic|Late Triassic|Geological Province: Maryborough Basin.||||||13-MAR-09
18119|Tiaro Coal Measures|62594|5|Briefly described|p546 Fig. 3, p559|Middle Jurassic|Late Triassic|Deltaic deposits. Age is Albian. Geological Province: Maryborough Basin||||||09-AUG-06
18119|Tiaro Coal Measures|63821|4|Described|p23|Early Jurassic||Of Duckinwilla Group. Overlie Myrtle Creek Sandstone; unconformably overlain by Grahams Creek Formation. Intruded by Mount Bauple Syenite. Geol.Prov:Nambour Basin. Comprises shale, siltstone, mudstone, coal, sandstone, volcanics and some limestone.||||||07-FEB-11
18119|Tiaro Coal Measures|64665|5|Briefly described|p53 Fig.2, p59.|Middle Jurassic|Early Jurassic|Northern Nambour Basin. Much of the coal has been naturally coked by plutonic intrusion, and heavily tectonised, dissected and boudinaged. No coal resource has been defined; there has been some recent (ie c.2008) exploration interest.||||Overlies Myrtle Creek Sandstone.||
18119|Tiaro Coal Measures|67402|4|Described|p165 tbl LPB1, p234-p237|Bathonian|Sinemurian|Maryborough Basin. Deposited in a fluvial-lacustrine environment.||Duckinwilla Group||Overlies the Myrtle Creek Sandstone. Unconformably overlain by the Grahams Creek Formation.|Shale, sandstone, siltstone, coal and ferruginous oolite.|
18119|Tiaro Coal Measures|68008|5|Briefly described|p238, p243|Early Jurassic|Early Jurassic|Maryborough Basin. Coeval with Evergreen Formation on the basis of a distinctive ooiltic ironstone marker bed.||||Upper part is correlated with Mulgildie Coal Measures.||
18119|Tiaro Coal Measures|68135|5|Briefly described|p50, p52 fig 2b|Bathonian||Northern Nambour Basin. Extensively intruded and varies considerably in rank, hence considered uneconomic. Previously mined for graphite. Contains plant macrofossils.||||Overlies Myrtle Creek Sandstone.|Interbedded coals, mudstones and sandstones and some oolitic ironstone beds.|15-SEP-17
18119|Tiaro Coal Measures|68679|6|Mentioned|p472|Middle Jurassic|Early Jurassic|Clarence-Moreton Basin.||||||
18119|Tiaro Coal Measures|69297|6|Mentioned|p370, p386|||Maryborough Basin.||||||
18119|Tiaro Coal Measures|69582|5|Briefly described|p48, p50-p51, p53|||Nambour Basin. Intersected in the GSQ Maryborough 16 hole. Thermal conductivity is provided. This unit has an estimated thickness of 800m.||Duckinwilla Group||Overlies the Myrtle Creek Sandstone. Unconformably overlain by the Grahams Creek Formation.|Sandstone, siltstone, shale and coal.|
18119|Tiaro Coal Measures|69594|5|Briefly described|p519, p544, p546-549, p561, p572|Middle Jurassic|Early Jurassic|Northern Nambour Basin. Contains coal seam up to 3m thick; no production yet. Exploration is being undertaken for coking coal deposits. RELATED UNITS (continued): Correlated with Walloon Coal Measures. Age-equivalent of Brighton beds, Ma Ma Creek Member and Westgrove Ironstone Member.||Duckinwilla Group.||Overlies Myrtle Creek Sandstone. Is overlain unconformably by Grahams Creek Formation or Maryborough Formation. Is intruded by Mount Bauple Syenite and Mount Urah Granodiorite. See COMMENTS for more.|Includes the distinctive Toarcian ferruginous oolite marker bed. Below that are two sandstone-siltstone-shale facies separated by a sandstone facies. The coal measures extend well beyond the oolite marker.|
18119|Tiaro Coal Measures|69599|5|Briefly described|p610, p620 Fig.8.21m|Jurassic|Jurassic|Grimes (1981, 1982). Nambour Basin. Tentatively correlated with strongly indurated sandstone and shale in a drillhole on the northern tip of Fraser Island.||||||
18119|Tiaro Coal Measures|72297|5|Briefly described|p700, p751, p761|Jurassic|Jurassic|Nambour Basin. Has received little attention for CSG potential. Elevated temperatures in the Basin have been attributed to insulation by this unit; implications for geothermal energy with few intrusives but thick coal measures.||||Equivalent to Raceview Formation.|Numerous thin, lenticular coal seams in a fluvial sandstone, silt and mudstone succession. The coal is widely heat affected by intrusives.|
18119|Tiaro Coal Measures|73422|6|Mentioned|p3, p5|Jurassic|Jurassic|Nambour Basin.||||Underlain by Myrtle Creek Formation. Overlain by Grahams Creek Formation.||
18119|Tiaro Coal Measures|73570|6|Mentioned|p914, p915 Fig.4, p917 Fig.5|Middle Jurassic|Middle Jurassic|Nambour Basin. See also Tiaro Formation p916.||||||
18135|Tidna Sandstone|23393|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Group.  Overlies Mullera Formation.||||||
18135|Tidna Sandstone|23937|6|Mentioned|p75 App. 1|||Of the South Nicholson Group.||||||
18135|Tidna Sandstone|26310|2|Defined|p4, 16, Table 1|Proterozoic|Proterozoic|Conformably overlies the Mullera Formation.  Quartzitic sandstone, siltstone, shale. Maximum Thickness: 1,200 feet. Type section in text. Overlain by: Colless Volcanics (unconformably), Mullera Formation? (conformably).||||||09-AUG-04
18135|Tidna Sandstone|32660|5|Briefly described|Table 5|||||||||
18135|Tidna Sandstone|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18135|Tidna Sandstone|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of South Nicholson Group.||||||
18135|Tidna Sandstone|45166|5|Briefly described|p33|||||||||
18135|Tidna Sandstone|65337|6|Mentioned|p50.|||Present only in LAWN HILL area.||Unit in Accident Subgroup.||||
18135|Tidna Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot.|Mesoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Mount Isa Block Time-Space Plot. South Nicholson Basin. Detrital [?zircon] ages: 1616 +/-16 Ma (Magee et al, in prep).||South Nicholson Group.|||Sandstone.|
18135|Tidna Sandstone|67539|6|Mentioned|p15 Fig.8, p16|||||Of the South Nicholson Group.||Underlain by the Mullera Formation.||
18135|Tidna Sandstone|68146|5|Briefly described|p196-197|||||Accident Subgroup.||Overlies Mullera Formation.||
18135|Tidna Sandstone|68575|4|Described|p3, p6-7, p27-36, p125, p128, p134|||South Nicholson Basin. Is stratigraphically 1000-2000m above the Burangoo Sandstone in the same Group. Whole rock Sm-Nd isotopic data and age (1616 Ma).|1614 +/- 13 Ma (maximum depositional age).|Topmost South Nicholson Group.||Gradationally overlies Mullera Formation.|Well-sorted, medium-grained, quartz-rich sandstone.|
18135|Tidna Sandstone|69434|5|Briefly described|p19:6|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960).||Accident Subgroup.||||12-JUL-16
18135|Tidna Sandstone|69591|4|Described|p52-54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Shallow-marine (?) deposits.|1616 +/- 16 Ma (MDA: Magee et al., in press).|Accident Subgroup.||Overlies Mullera Formation.|Sandstone.|
18135|Tidna Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Tidna. South Nicholson Basin.||||||
18135|Tidna Sandstone|71369|4|Described|p1, p5-6, p23, p37, p43-44, p49|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960), who revised the definition of Mullera Formation of Carter et al. (1961) [sic] by raising this unit to Formation status rather than the uppermost Member of Mullera Formation. South Nicholson Basin. Up to 350m thick. Progradational deposits. Marks the end of deposition in the Basin.||Accident Subgroup.||Conformably and gradationally overlies Mullera Formation.|Medium-grained, well-sorted, thick-bedded cross-bedded sandstone. Possible gypsum pseudomorphs.|20-FEB-18
18135|Tidna Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1614+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
18135|Tidna Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, cross-bedded sandstone.|26-NOV-19
18135|Tidna Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Accident Subgroup.||Overlain by Colless Volcanics. Underlain by Mullera Formation.|Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, corss-bedded sandstone.|
18135|Tidna Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Accident Subgroup.||Overlain by Colless Volcanics. Underlain by Mullera Formation.|Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, corss-bedded sandstone.|
18135|Tidna Sandstone|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, corss-bedded sandstone.|
18135|Tidna Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, cross-bedded sandstone|
18135|Tidna Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, cross-bedded sandstone|
18135|Tidna Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, cross-bedded sandstone|
18135|Tidna Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Accident Subgroup.|||Thin-bedded, very fine to fine-grained sandstone passing upwards into thick-bedded, medium-grained, well-sorted, cross-bedded sandstone|
18135|Tidna Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as located in the central and eastern parts of the South Nicholson Basin.||||Overlies Mullera Formation.||
18135|Tidna Sandstone|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin.||||Shown as overlying Mullera Formation.||
18135|Tidna Sandstone|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the central part of the South Nicholson Basin.||||Overlies Mullera Formation.|Includes sandstone.|
18135|Tidna Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||Accident Subgroup, South Nicholson Group||Underlain by Mullera Formation.||
18135|Tidna Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||||Underlain by Mullera Formation.||
18135|Tidna Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin.||Accident Subgroup, South Nicholson Group||Underlain by Mullera Formation.||
18166|Timberoo Member|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Marraba Volcanics (Malbon Group). Siltstone, quartzite, sandstone, metabasalt, andesite.||||||
18166|Timberoo Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18166|Timberoo Member|30530|2|Defined|p516|Precambrian|Precambrian|Also mention p515.||||||01-FEB-07
18166|Timberoo Member|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18166|Timberoo Member|38350|6|Mentioned|p10|||||||||
18166|Timberoo Member|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18166|Timberoo Member|39496|5|Briefly described|p5|||||||||
18166|Timberoo Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
18166|Timberoo Member|41791|5|Briefly described|p248|||See also p249.||||||01-FEB-07
18166|Timberoo Member|45161|6|Mentioned|p40|||||||||
18166|Timberoo Member|45166|5|Briefly described|p20|||||||||
18166|Timberoo Member|49041|6|Mentioned|Table 4|||||||||
18166|Timberoo Member|50100|5|Briefly described|p17|Statherian|Statherian|Of the Marraba Volcanics.  Geological Province: Eastern Fold Belt.||||||20-JAN-05
18166|Timberoo Member|63866|6|Mentioned|p62, p65|||Mitakoodi Anticline.||Marraba Volcanics||||
18166|Timberoo Member|67323|5|Briefly described|GIS attrib tbl, p16|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Eastern Fold Belt, Mount Isa area; Leichhardt Superbasin.||Marraba Volcanics.|||Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone|
18166|Timberoo Member|68146|5|Briefly described|p78|||||Marraba Volcanics.|||Fine-grained metasedimentary rocks.|
18166|Timberoo Member|68575|5|Briefly described|p47, p126|||Mitakoodi Domain.||Marraba Volcanics.|||Fine-grained metasedimentary rocks.|
18166|Timberoo Member|68732|6|Mentioned|p165|||Of the Myally Supersequence.||||Overlies Mount Start Member.||01-DEC-17
18166|Timberoo Member|69056|6|Mentioned|Time-Space plot sheet|Statherian|Statherian|||Marraba Volcanics.||||
18166|Timberoo Member|70355|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Overlies Mount Start Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone. A metabasalt sub-unit is mapped separately.|
18166|Timberoo Member|70356|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Marraba Volcanics.||Overlies Mount Start Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone. A metabasalt sub-unit is mapped separately.|
18166|Timberoo Member|71799|6|Mentioned|p154|||||Marraba Volcanics||||
18166|Timberoo Member|72682|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Overlies Mount Start Member, Cone Creek Metabasalt Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
18166|Timberoo Member|72683|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain.||Marraba Volcanics||Overlies Mount Start Member, Cone Creek Metabasalt Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
18166|Timberoo Member|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Marraba Volcanics||Overlying Cone Creek Metabasalt Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
18166|Timberoo Member|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Mitakoodi Domain. Shown as older than the the Wonga-Burstall Event (c. 1740 Ma).||Marraba Volcanics||Overlying Cone Creek Metabasalt Member.|Siltstone and labile sandstone; minor limestone and calcareous to dolomitic siltstone.|
18177|Timbury Hills Formation|22768|6|Mentioned|p153,159||Early Devonian|||||||
18177|Timbury Hills Formation|22857|5|Briefly described|p153|Early Devonian|?Early Devonian|Possibly correlates with Cobar Supergroup. See also p165 Fig. 16.6.||||||
18177|Timbury Hills Formation|24069|5|Briefly described|p282|Late Devonian|Late Devonian|Geological Province: Surat Basin.||||||
18177|Timbury Hills Formation|24075|5|Briefly described|p393|||Geological Province: Drummond Basin.||||||
18177|Timbury Hills Formation|29413|6|Mentioned|p295|||||||||
18177|Timbury Hills Formation|29488|6|Mentioned|p7|||||||||
18177|Timbury Hills Formation|29721|6|Mentioned|p69|||||||||
18177|Timbury Hills Formation|30692|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
18177|Timbury Hills Formation|30699|6|Mentioned|p55|||Map||||||
18177|Timbury Hills Formation|31369|6|Mentioned|p11|||Devonian||||||
18177|Timbury Hills Formation|31999|5|Briefly described|p136|||Table 1||||||
18177|Timbury Hills Formation|32578|5|Briefly described|p347|||Dev. Stratigraphy Roma area||||||
18177|Timbury Hills Formation|32712|6|Mentioned|Table 1|||||||||
18177|Timbury Hills Formation|33059|4|Described|Table 1|||Dev.||||||
18177|Timbury Hills Formation|33530|5|Briefly described|Table 1|||||||||
18177|Timbury Hills Formation|33672|6|Mentioned|p41|||||||||
18177|Timbury Hills Formation|33745|6|Mentioned|p205|||Devonian.||||||
18177|Timbury Hills Formation|34133|6|Mentioned|p29|||||||||
18177|Timbury Hills Formation|34212|6|Mentioned|p2|||See also P3. Devonian.||||||
18177|Timbury Hills Formation|36104|6|Mentioned|p122|||||||||
18177|Timbury Hills Formation|36233|5|Briefly described|Table 1|||||||||
18177|Timbury Hills Formation|36739|6|Mentioned|p22|||||||||
18177|Timbury Hills Formation|37450|6|Mentioned|p366|||||||||
18177|Timbury Hills Formation|37724|6|Mentioned|Fig.5|||||||||
18177|Timbury Hills Formation|39273|6|Mentioned|Fig. 2|||||||||
18177|Timbury Hills Formation|40030|6|Mentioned|p139|||||||||
18177|Timbury Hills Formation|40541|3|Fully described|p104|||||||||
18177|Timbury Hills Formation|40666|4|Described|p353|||||||||
18177|Timbury Hills Formation|40787|4|Described|p341|||||||||
18177|Timbury Hills Formation|41210|6|Mentioned|Fig.16|||||||||
18177|Timbury Hills Formation|41725|6|Mentioned|p403|||||||||
18177|Timbury Hills Formation|42031|4|Described|p766|||||||||
18177|Timbury Hills Formation|42041|6|Mentioned|Fig.4 P223|||||||||
18177|Timbury Hills Formation|42634|6|Mentioned|Fig.7 P26|||||||||
18177|Timbury Hills Formation|42987|4|Described|p19|||says unit can't have Formation status under the Australian Code of Stratigraphic Nomenclature||||||
18177|Timbury Hills Formation|42996|5|Briefly described|p14|||||||||
18177|Timbury Hills Formation|43000|5|Briefly described|p106|||||||||
18177|Timbury Hills Formation|43003|5|Briefly described|p167|||||||||
18177|Timbury Hills Formation|43007|5|Briefly described|Fig.2,p255|||||||||
18177|Timbury Hills Formation|43008|5|Briefly described|map legend|||||||||
18177|Timbury Hills Formation|43213|6|Mentioned|p61-63|Devonian|Devonian|Finlayson et al.(1990). Near the W edge of this unit, the Foyleview Geosuture - a major W-dipping detachment - marks the E edge of the Thomson Fold Belt.||||||
18177|Timbury Hills Formation|43461|14|Not recorded|p616,617|||Equivalent to Telemon and Mount Rankin Formations||||||
18177|Timbury Hills Formation|44023|5|Briefly described|Tb.2,p6||Late Devonian|||||||
18177|Timbury Hills Formation|44091|14|Not recorded|p39||Carboniferous|||||||
18177|Timbury Hills Formation|44115|14|Not recorded|p17-19,24|||||||||
18177|Timbury Hills Formation|44116|14|Not recorded|p24,28|||||||||
18177|Timbury Hills Formation|44118|14|Not recorded|Map Legend||Late Devonian|||||||
18177|Timbury Hills Formation|44163|14|Not recorded|p11|||||||||
18177|Timbury Hills Formation|44169|2|Defined|Tb.1,6,7,map|||||||||
18177|Timbury Hills Formation|44170|4|Described|p5-7,30,Tb.1||Late Devonian|||||||
18177|Timbury Hills Formation|44172|14|Not recorded|p1326,1329,1331,Tb.1||Devonian|||||||
18177|Timbury Hills Formation|44173|14|Not recorded|p112|||||||||
18177|Timbury Hills Formation|44422|14|Not recorded|p148,151-153,155||Devonian|Basement.||||||
18177|Timbury Hills Formation|44423|14|Not recorded|p20-22|||(Dev?Early Carb?Perm?)||||||
18177|Timbury Hills Formation|44585|14|Not recorded|p45-Fig.2|||||||||
18177|Timbury Hills Formation|44610|14|Not recorded|Fig.7|||||||||
18177|Timbury Hills Formation|44627|14|Not recorded|p139|||||||||
18177|Timbury Hills Formation|44636|14|Not recorded|p162|Early Devonian|Late Silurian|||||||
18177|Timbury Hills Formation|44646|14|Not recorded|p1|||Tarrawanga No.2.||||||
18177|Timbury Hills Formation|44686|14|Not recorded|p1-6,16|||||||||
18177|Timbury Hills Formation|44701|14|Not recorded|Tb.VI|||Dirinda 1||||||
18177|Timbury Hills Formation|44787|14|Not recorded|Tb.p123,125-127,diag||Late Devonian|||||||
18177|Timbury Hills Formation|44842|14|Not recorded|p13|||||||||
18177|Timbury Hills Formation|44897|14|Not recorded|p8,16|||||||||
18177|Timbury Hills Formation|45071|6|Mentioned|p45|||||||||
18177|Timbury Hills Formation|45095|6|Mentioned|p4|||||||||
18177|Timbury Hills Formation|45110|4|Described|p25|||See also P66.||||||
18177|Timbury Hills Formation|46989|6|Mentioned|p215|||||||||
18177|Timbury Hills Formation|48585|4|Described|p1,7,12-15,Pl.1|||||||||
18177|Timbury Hills Formation|48600|14|Not recorded|Plate 3|||||||||
18177|Timbury Hills Formation|48606|14|Not recorded|p3,5,6,11,13,14,22|||(H/55-8 ; G/55-12). Pl.1 sh.2, Pl.2.||||||
18177|Timbury Hills Formation|48611|14|Not recorded|p8,16,Fig.2|||||||||
18177|Timbury Hills Formation|48920|6|Mentioned|p85|||||||||
18177|Timbury Hills Formation|64855|4|Described|p16 Fig.2, p18-22, 36|Early Carboniferous|Devonian|Fine grained, quartz rich metasedimentary rocks of the Thomson and Lachlan fold belts, forming part of the basement to the Bowen Basin. Min age based on the Upper Devonian/Lower Carboniferous Roma granites that intrude this formation.||||||22-FEB-10
18177|Timbury Hills Formation|64856|5|Briefly described|p43, p46, p63, p74|Devonian|Devonian|Unconformably underlies Combarngo Volcanics,  Arbroath beds, Muggleton Formation. Considered part of source for Showgrounds Sandstone.|| ||||29-NOV-17
18177|Timbury Hills Formation|65115|6|Mentioned|p407|Devonian|Devonian|Intercepted in  AAO Glentulloch 1.||||||
18177|Timbury Hills Formation|67669|5|Briefly described|p11-12,22-23|Late Carboniferous|Late Carboniferous|Of Bowen Basin. Part of the basement assemblage to the Bowen Basin. Low-grade metasedimentary rocks in the Roma region. Intersected in Myall Creek-1 borehole at 2.1 km depth, and represents basement as modelled on Line 270.||||Overlain by Reid Dome beds, Lizzie Creek, Cmbarngo and Bulgonunna volcanics. Underlain by, and laterally grades into Kuttung Formation. Intruded by Roma granites.||
18177|Timbury Hills Formation|68679|5|Briefly described|p371-372|Devonian|Devonian|Murray (1994). Basement to the Bowen Basin in the Roma area. Possibly turbidites.||||Is intruded by the Roma granites.|Includes quartzose sandstone, siltstone and cleaved argillite. Metamorphosed to lower greenschist grade.|
18177|Timbury Hills Formation|68731|5|Briefly described|p164, p168, p213 Fig 3.118|Devonian|Devonian|Generally steeply dipping with usually a single slaty cleavage and regional low-grade metamorphism.|||||Consists of turbiditic quartzose sandstone and mudstone deposited in a deep-marine environment.|
18177|Timbury Hills Formation|69582|5|Briefly described|p32, p34-p35, p38|Devonian|Devonian|Surat Basin. Forms basement in the Roma Shelf. Undergone folding producing upright, tight to isoclinal folds. Metamorphosed to greenschist facies. Deposited in a deep marine environment. Intruded by the Roma granites. Interpreted to extend to at least 5km depth.|||||Steeply dipping metasediments including turbiditic quartzose sandstone and mudstone.|
18177|Timbury Hills Formation|69592|6|Mentioned|p229|Devonian||Roma area. An extensive, subsurface, metasedimentary unit; intruded by the c.356 Ma Roma granites.||||||
18177|Timbury Hills Formation|70033|6|Mentioned|p1-2|||See informal Timbury Hills formation for Geochron age.||||||
18177|Timbury Hills Formation|70673|4|Described|p3, p10, p62, p64, p66-70|Devonian|Devonian|Roma Shelf. Metamorphosed, deep-marine sedimentary rocks. Devonian age from plant fossils. Metamorphosed at 360 +/- 8 Ma. Previous determination gives a MDA of 417.6 +/- 3.1 Ma (Kositcin et al., 2015).|401 +/- 7 Ma (maximum depositional age).|||Intruded by Roma Granites.|Interbedded sandstone, siltstone and argillite metamorphosed to lower greenschist facies. Includes garnet-muscovite-biotite paragneiss. Has volcanic horizon(s).|
18177|Timbury Hills Formation|71592|5|Briefly described|Appendix A.|||Roma Shelf, Surat Basin. Metamorphosed at 360 +/- 8 Ma (U-Pb zircon SHRIMP).|401+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Gneiss.|
18177|Timbury Hills Formation|71965|5|Briefly described|p912,914|Middle Devonian|Early Devonian|Of Roma Shelf. Proposed to be correlable to Glenroy Formation in the Thomson Orogen. Underwent folding and metamorphism.||||||
18177|Timbury Hills Formation|72522|5|Briefly described|p98-104, p105, 107.||Early Devonian|Eastern Lachlan Orogen. Maximum depositional age determined from AAO Glenroy 1, in Roma region. Previous U-Pb SHRIMP max. dep. age dating from  a metasandstone in AAO Timbury Hills 2: 420+/-4 Ma. Another sample dated herein (2172124) at 388+/-5 Ma from UOD Weribone 1 , and originally interpreted as Timbury Hills Formation, is now interpreted as a younger Thomson Orogen unit.|412+/-6 Ma U-Pb SHRIMP.(Max dep age)||||Dated sample is grey-green, medium-grained quartzite.|24-FEB-21
18177|Timbury Hills Formation|73600|6|Mentioned|p203|||Roma Shelf. Characterised by the Pacific-Gondwanan detrital zircon ages.||||||
18185|Timothy Creek Sandstone Member|24419|5|Briefly described|p16|Proterozoic|Proterozoic|Main sedimentary unit in Jayah Creek Metabasalt (Haslingden Group).||||||09-MAR-05
18185|Timothy Creek Sandstone Member|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Jayah Creek Metabasalt.||||||25-AUG-04
18185|Timothy Creek Sandstone Member|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18185|Timothy Creek Sandstone Member|38658|6|Mentioned|p153|||||||||
18185|Timothy Creek Sandstone Member|45161|5|Briefly described|Table 2|||||||||
18185|Timothy Creek Sandstone Member|45166|5|Briefly described|p16|||||||||
18185|Timothy Creek Sandstone Member|49009|2|Defined|p48|Precambrian|Precambrian|Mapped as Eastern Creek Volcanics by Noakes and others (1959).||||||11-DEC-06
18185|Timothy Creek Sandstone Member|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Meta-arenite; minor metasiltstone, quartzite, metabasalt.||||||
18185|Timothy Creek Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.||Lower Haslingden Group|||Quartz and feldspathic sandstone.|
18192|Tinaroo Granite|23423|5|Briefly described|p311 Table 7.4||Early Permian|S-type granite. Also see p245. Age: 268-283 Ma, 253-285 Ma. Similar to Whypalla Supersuite. Tinaroo Supersuite.||||||
18192|Tinaroo Granite|23497|5|Briefly described|Table 1||Early Permian|of Tinaroo Supersuite, Kennedy Province. Intrudes Hodgkinson Formation rocks and Emerald Creek Microgranite.||||||
18192|Tinaroo Granite|23506|5|Briefly described|Map Legend||Early Permian|Age: ~282+/-9Ma Rb-Sr. of Tinaroo Supersuite.||||||
18192|Tinaroo Granite|23507|5|Briefly described|Map Legend||Early Permian|||||||
18192|Tinaroo Granite|23513|5|Briefly described|Map legend||Permian|Palaeozoic Intrusive No. 390. S-Type.||||||
18192|Tinaroo Granite|23616|4|Described|p78||Permian|Age: 268-283 Ma (K-Ar) and 253-285 Ma (Rb-Sr). Intrudes Emerald Creek Microgranite. Of Tinaroo Supersuite. Tinaroo Batholith.||||||
18192|Tinaroo Granite|24086|6|Mentioned|p321|||||||||
18192|Tinaroo Granite|24213|5|Briefly described|p776 Fig. 1|Permian|Early Permian|||||||
18192|Tinaroo Granite|39689|6|Mentioned|p58|||||||||
18192|Tinaroo Granite|39997|6|Mentioned|p165|||||||||
18192|Tinaroo Granite|42625|5|Briefly described|Map legend|Late Permian|Early Permian|||||||
18192|Tinaroo Granite|42810|2|Defined|Table 1 P16|Late Permian|Early Permian|see also P24. Age: early Early Permian to early Late Permian||||||
18192|Tinaroo Granite|43060|5|Briefly described|p108|||of Tinaroo Supersuite. Radiometric ages of 253-285 Ma||||||
18192|Tinaroo Granite|43259|4|Described|Appendix 1,p43.||Permian|Age is 268-283 Ma.||||||
18192|Tinaroo Granite|60425|3|Fully described|p56 Tb. 4, p181|Early Permian|Early Permian|Of the Tinaroo Supersuite. Age: ~280Ma (Rb-Sr). Intruded part of Hodgkinson Formation and Emerald Creek Microgranite. White to pale grey, medium-grained, slightly to moderately porphyritic, biotite granite. S-type.||||||07-FEB-11
18192|Tinaroo Granite|69079|6|Mentioned|p48|||The contact aureole of this unit hosts the Waitemata gold deposit, but mineralisation appears not to be associated with the Granite.||||||
18192|Tinaroo Granite|69592|5|Briefly described|p242, p249 Fig.4.34|Permian|Permian|||||Partly stopes out Emerald Creek Microgranite.||
18192|Tinaroo Granite|69593|5|Briefly described|p477, p479, p511|||Daintree Subprovince, Kennedy Igneous Association. Crops out over ~305 km2 at Lamb Range, SW of Cairns. Age poorly constrained. Sm-Nd isotope data tabulated.|280 Ma.|Tinaroo Suite.|||S-type. Slightly to moderately porphyritic, biotite granite, traces of late garnet.|
18192|Tinaroo Granite|72983|4|Described|p1, p3, p7, p19, p22-23, p25-27|Kungurian|Kungurian|Kennedy Igneous Association. Hodgkinson Province, southern. Cairns region. An irregular, composite body. Previous K-Ar ages range from 268 to 283 Ma. Previous Rb-Sr age estimates range from 253 to 285 Ma. These may reflect partial to complete resetting. Similar in age to granites of the Whypalla Supersuite. Occurs within the same geographic belt as the Whypalla Supersuite granites; thus, future work may indicate that it is part of that supersuite as opposed to either the Tinaroo Suite or Tinaroo Supersuite. Only key difference from those granites is more primative eNd values (-2.3). Suspected coeval with Collins Weir Rhyolite, Hope Vale Granite, Featherbed Volcanic Group and Nychum Volcanics.|281.2 +/- 1.4 Ma SHRIMP U-Pb|Tinaroo Suite / Tinaroo Supersuite|||Includes porphyritic muscovite-biotite monzogranite.|
18193|Tinbeerwah rhyolite|39969|6|Mentioned|p39|||||||||
18193|Tinbeerwah rhyolite|40542|6|Mentioned|p98|||||||||
18204|Tingalpa Formation|30302|6|Mentioned|p415|||Refers to Houston(1965)||||||
18204|Tingalpa Formation|30455|6|Mentioned|p7|||See also P12,21. Triassic age||||||
18204|Tingalpa Formation|30458|6|Mentioned|p3|||Triassic age||||||
18204|Tingalpa Formation|30460|6|Mentioned|p12|||See also P13,14,22. Triassic age||||||
18204|Tingalpa Formation|30465|6|Mentioned|p4|||||||||
18204|Tingalpa Formation|30466|6|Mentioned|p5|||Triassic age||||||
18204|Tingalpa Formation|30470|6|Mentioned|p457|||||||||
18204|Tingalpa Formation|30517|6|Mentioned|p436|||||||||
18204|Tingalpa Formation|30785|6|Mentioned|p398|||||||||
18204|Tingalpa Formation|32136|6|Mentioned|p5|||Miospores||||||
18204|Tingalpa Formation|35053|5|Briefly described|p35|||||||||
18204|Tingalpa Formation|38074|5|Briefly described|Table 1|||||||||
18204|Tingalpa Formation|38373|6|Mentioned|p615|||||||||
18204|Tingalpa Formation|40579|6|Mentioned|Map legend|late Carnian|late Carnian|||||||
18204|Tingalpa Formation|40623|5|Briefly described|p7|||||||||
18204|Tingalpa Formation|42316|5|Briefly described|p18|||||||||
18204|Tingalpa Formation|43076|5|Briefly described|p7|||||||||29-SEP-05
18204|Tingalpa Formation|43921|14|Not recorded|p315-323|||||||||
18204|Tingalpa Formation|43923|6|Mentioned|p5||Triassic|||||||
18204|Tingalpa Formation|44029|14|Not recorded|p158|Late Triassic|Middle Triassic|Middle - Late Triassic plant.||||||
18204|Tingalpa Formation|44030|2|Defined|p115,117,118,120,||Late Triassic|p12-129,132-135,140,141||||||
18204|Tingalpa Formation|44687|2|Defined|p221-222|Late Triassic|Middle Triassic|?Equivalent of Tivoli Formation. Previously included in Brisbane Tuffs.||||Disconformably overlies  Brisbane Tuff,disconformably overlain by Moorooka Formation. In apparent faulted contact with Brighton Beds.||21-MAR-13
18204|Tingalpa Formation|44703|14|Not recorded|Map|Late Triassic|Middle Triassic|||||||
18204|Tingalpa Formation|44708|14|Not recorded|p4,5,14,19,23,Sh.1,3||Middle Triassic|Building stone. Formerly called Ipswich Coal Measures. Sheet 5.||||||
18204|Tingalpa Formation|68679|5|Briefly described|p392, p394|Late Triassic|Late Triassic|Ipswich Basin: Brisbane/Beenleigh/offshore. Is well displayed in St Helena 1. Fossils include conchostracans, bivalves, fish scales and tracks of labyrinthodonts and dinosaurs (elaborated).||||Equivalent to Tivoli Formation (Ipswich area).||
18232|Tirrawarra Sandstone|13497|3|Fully described|iv, vi, viii, x, xii, p47-p48, |Asselian|Stephanian|Cooper Basin. Previously the Tirrawarra Formation of Kapel (1972) before being renamed by Gatehouse in the same year. The name is derived from the Tirrawarra Swamp. A reference section is mentioned. This formation is widespread but thin, only reaching 75m thick. Hosts the largest Permian oil accumulation in the Cooper Basin. Deposited in a braidplain or deltal environment. Reservoir characteristics discussed. See also p54, p61, p64-p66, p69 fig 6.1, p75-p78, p81, p84-90, p119, p122, p138 fig 8.17, p139 fig 8.18, p141, p146,  p150, p153,  p157-p160, p173, p177, p181-p184, p188-p190, p204, p208, p216.||Gidgealpa Group||Interfingers with or unconformably overlies the Merrimelia Formation. Interfingers with and is overlain by the Patchawarra Formation.|Brown and white, fine to coarse-grained, moderately well sorted sandstone with minor shale interbeds and rare thin coal seams and stringers.|
18232|Tirrawarra Sandstone|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Cooper Basin||||||
18232|Tirrawarra Sandstone|22527|4|Described|p 2, 3, 4,||Early Permian|Replaced by Big Lake Suite, in Moomba Field.  Informally termed "Tirrawarra Conglomerate".||||||14-APR-08
18232|Tirrawarra Sandstone|22839|6|Mentioned|P33|||||||||
18232|Tirrawarra Sandstone|22883|6|Mentioned|P29|||Underlying unit is Merrimelia Formation||||||
18232|Tirrawarra Sandstone|23154|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province - Cooper Basin.  Parent - Gidgealpa Group.||||||
18232|Tirrawarra Sandstone|23155|4|Described|p14 & p17|Early Permian|Late Carboniferous|Sparse spore-pollen assemblages indicate that the unit is predominantly Early Permian in age but may range downward into the Late Carboniferous where interbedded with the Merrimelia Formation.  Thickness distribution in the unit is variable (see p 17).||||||
18232|Tirrawarra Sandstone|23375|4|Described|Fig2 p265,285||Asselian|In the Cooper Basin.||||||17-JAN-08
18232|Tirrawarra Sandstone|24199|5|Briefly described|p512 Fig.2|Early Permian|Early Permian|Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|24204|5|Briefly described|p262, 263 Fig.4, p284|Early Permian|Early Permian|Mainly discussed in terms of Tirrawarra Sandstone equivalent. Geological Province: Cooper Basin.||||||31-MAR-05
18232|Tirrawarra Sandstone|24212|5|Briefly described|p67 Fig. 3p|Early Permian|Early Permian|Age: >290Ma.  Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|29387|6|Mentioned|Table 2|||Refers to Gatehouse 1972.||||||
18232|Tirrawarra Sandstone|29721|6|Mentioned|Table 137|||||||||
18232|Tirrawarra Sandstone|30540|6|Mentioned|p65|||Produces gas in Gidgealpa No.7||||||
18232|Tirrawarra Sandstone|30544|6|Mentioned|p53|||||||||
18232|Tirrawarra Sandstone|30873|3|Fully described|p14|||Refers Kapel (1972). Previously Tirrawarra Formation.||||||30-JUN-08
18232|Tirrawarra Sandstone|32696|6|Mentioned|Fig.4|||Refers Gatehouse (1972)||||||
18232|Tirrawarra Sandstone|33074|6|Mentioned|p260|||||||||
18232|Tirrawarra Sandstone|33331|6|Mentioned|p41|||||||||
18232|Tirrawarra Sandstone|33489|6|Mentioned|Fig.2|||Refers Kapel (1972) & Gatehouse (1972)||||||
18232|Tirrawarra Sandstone|35067|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|35068|6|Mentioned|Fig.3|||Discussed P54.||||||
18232|Tirrawarra Sandstone|35457|6|Mentioned|Fig.4|||Biostratigraphic relationships. See also P627.||||||
18232|Tirrawarra Sandstone|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
18232|Tirrawarra Sandstone|35845|4|Described|p24|||Lithology and depositional environments. See also p42.||||||17-JAN-08
18232|Tirrawarra Sandstone|36099|6|Mentioned|p191|||||||||
18232|Tirrawarra Sandstone|36910|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|36917|6|Mentioned|Fig.1|||||||||
18232|Tirrawarra Sandstone|37703|6|Mentioned|p2240|||||||||
18232|Tirrawarra Sandstone|37855|6|Mentioned|p4|||See also Fig.2.||||||
18232|Tirrawarra Sandstone|37917|6|Mentioned|Fig.2|||||||||
18232|Tirrawarra Sandstone|38977|6|Mentioned|Fig.1|||||||||
18232|Tirrawarra Sandstone|39252|5|Briefly described|p13|||||||||
18232|Tirrawarra Sandstone|39254|5|Briefly described|p45|||||||||
18232|Tirrawarra Sandstone|39261|6|Mentioned|Fig. 9|||||||||
18232|Tirrawarra Sandstone|39265|6|Mentioned|Fig. 3|||||||||
18232|Tirrawarra Sandstone|39276|6|Mentioned|Fig. 2|||||||||
18232|Tirrawarra Sandstone|39445|5|Briefly described|Table 7|||See also P92 & Table 8||||||
18232|Tirrawarra Sandstone|39478|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|39494|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|40030|6|Mentioned|p131|||See also Fig.3||||||
18232|Tirrawarra Sandstone|40249|6|Mentioned|p45|||||||||
18232|Tirrawarra Sandstone|40544|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|41099|6|Mentioned|p190|||||||||
18232|Tirrawarra Sandstone|41123|6|Mentioned|p180|||||||||
18232|Tirrawarra Sandstone|41131|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|41164|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|41166|4|Described|p379|||||||||
18232|Tirrawarra Sandstone|41183|6|Mentioned|p307|||See also Fig.3||||||
18232|Tirrawarra Sandstone|41189|6|Mentioned|Fig.4|||||||||
18232|Tirrawarra Sandstone|41198|6|Mentioned|Table 1|||||||||
18232|Tirrawarra Sandstone|41214|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|41221|6|Mentioned|p389|||||||||
18232|Tirrawarra Sandstone|41247|6|Mentioned|Fig.5|||||||||
18232|Tirrawarra Sandstone|41267|6|Mentioned|p262|||||||||
18232|Tirrawarra Sandstone|41288|6|Mentioned|p156|||||||||
18232|Tirrawarra Sandstone|41595|6|Mentioned|Fig. 5|||||||||
18232|Tirrawarra Sandstone|41720|6|Mentioned|p370|||||||||
18232|Tirrawarra Sandstone|42085|6|Mentioned|Fig.2 P374|||||||||
18232|Tirrawarra Sandstone|42395|5|Briefly described|Fig.13 P83|||||||||
18232|Tirrawarra Sandstone|42547|4|Described|p81|||||||||
18232|Tirrawarra Sandstone|42746|5|Briefly described|p3|||Cooper Basin||||||
18232|Tirrawarra Sandstone|42999|5|Briefly described|Table 2,p90||Early Permian|||||||
18232|Tirrawarra Sandstone|43018|5|Briefly described|Table 1,p386|||||||||
18232|Tirrawarra Sandstone|43105|5|Briefly described|Fig.7,p13.|||||||||
18232|Tirrawarra Sandstone|43570|5|Briefly described|Fig.2,p535,541|Early Permian|Late Carboniferous|||||||
18232|Tirrawarra Sandstone|43628|6|Mentioned|Fig.3||Early Permian|||||||
18232|Tirrawarra Sandstone|43711|6|Mentioned|p19||Early Permian|||||||
18232|Tirrawarra Sandstone|44133|4|Described|p65 Fig. 8.3, 83, 84|Sakmarian|Asselian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Average Thickness: ~70m. Conformably underlies Patchawarra Formation.||||||
18232|Tirrawarra Sandstone|46849|6|Mentioned|Fig. 7|||||||||
18232|Tirrawarra Sandstone|48995|6|Mentioned|Fig.3|||||||||
18232|Tirrawarra Sandstone|60386|6|Mentioned|p296|Sakmarian|Sakmarian|Cooper Basin. Non-marine.||||||
18232|Tirrawarra Sandstone|60717|5|Briefly described|p40 Fig. 2, p41|Asselian|Late Carboniferous|Probably supersedes Tirrawarra Formation? Of the Gidgealpa Group. Thickness: 75m. Geological Province: Cooper Basin.||||||31-JAN-08
18232|Tirrawarra Sandstone|61015|6|Mentioned|p44|||In the Cooper-Eromanga Basins.||||||
18232|Tirrawarra Sandstone|61250|6|Mentioned|p45|||Contains petroleum systems. Geological Province: Cooper Basin.||||||
18232|Tirrawarra Sandstone|61614|6|Mentioned|p290, p294, p295, p290 Fig. 2|||Of Gidgealpa Group. Geological Province: Cooper Basin.||||||17-MAR-09
18232|Tirrawarra Sandstone|61615|5|Briefly described|p302, p303, p302 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Overlain by Patchawarra Formation. Geological Province: Cooper Basin. Glacial or braided fluvial deposits.||||||22-AUG-18
18232|Tirrawarra Sandstone|61616|6|Mentioned|p330 Fig. 2|Early Permian|Late Carboniferous|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||31-MAR-09
18232|Tirrawarra Sandstone|62046|5|Briefly described|p125 Fig. 2|Permian|Carboniferous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
18232|Tirrawarra Sandstone|62376|5|Briefly described|p84|Early Permian|Late Carboniferous|Geological Province: Pedirka Basin.||||||09-FEB-10
18232|Tirrawarra Sandstone|62537|6|Mentioned|p191 Fig.2. |Early Permian||Cooper Basin.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|62730|5|Briefly described|p352 Fig. 1|Early Permian|Late Carboniferous|Geological Province: Cooper Basin.||||||14-APR-08
18232|Tirrawarra Sandstone|62759|5|Briefly described|p1|||Geological Province: Cooper Basin. Correlates with a glacigene sandstone at base of Purni Formation in the Perdika Basin.||||||05-FEB-08
18232|Tirrawarra Sandstone|63832|5|Briefly described|p131 fig 2, p135|Cisuralian|Cisuralian|Of Cooper Basin. Is mentioned on p135 as the abbreviated [and mis-spelt] Tirrawarra-Merimelia Formations. Thick succession of continental proglacial and possibly subglacial facies.||||Overlies and interfingers with Merrimelia Formation.|Continental proglacial and possibly subglacial facies.|14-DEC-17
18232|Tirrawarra Sandstone|63978|2|Defined|p10, Fig. 3|Early Permian|Early Permian|Of Gidgealpa Gp.Conformable over Merrimelia Fm; conformable under Patchawarra Fm; intertongues with both. Thick: 44m. Mainly fine- to coarse-gr.+ pebbly sandstone (massive)+ interbeds of conglomerate+ minor interbeds of carbonaceous siltst, shale+coal||||||07-FEB-11
18232|Tirrawarra Sandstone|64048|5|Briefly described|p65|Early Permian|Early Permian|Contains very small reserves of oil.||||||07-FEB-11
18232|Tirrawarra Sandstone|64197|6|Mentioned|p625 Fig.1c|Permian|Carboniferous|Cooper Basin.||||Underlies the Patchawarra Formation, overlies the Merrimelia Formation.||
18232|Tirrawarra Sandstone|64631|5|Briefly described|p44 Fig.2, p49.|Sakmarian|Asselian|Cooper Basin. Contains thick successions of continental proglacial facies. Some biostratigraphic age control. Shown with time transgressive base.||||Overlies Merrimelia Formation. Overlain by Patchawarra Sandstone.||
18232|Tirrawarra Sandstone|64665|5|Briefly described|p53 Fig.2, p56.|Early Permian|Early Permian|Cooper Basin. Hydrocarbon reservoirs are thought to have been charged from Patchawarra Formation.||||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|64778|6|Mentioned|p13|Carboniferous|Carboniferous|Pedirka Basin.||||||
18232|Tirrawarra Sandstone|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Early Permian|Late Carboniferous|Geological province: Pedirka Basin, Cooper Basin. Glacial outwash deposits.||||||09-APR-13
18232|Tirrawarra Sandstone|65489|5|Briefly described|p11, p15-16, p47-49, p55, p96, p131-132|Asselian|Late Carboniferous|See also p143. Cooper Basin. 75m thick. In 1970 Bridge Oil announced flow of light crude oil from Tirrawarra 1. Gas and oil reservoir accounting for 6% and 90% respectively of the Basin's production.||Unit in Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.|Braided fluvial to fan-delta deposits.|
18232|Tirrawarra Sandstone|65925|5|Briefly described|Appendix 2.||||||||Conglomerate, medium- to coarse-grained sandstone, mudstone; minor coal.|
18232|Tirrawarra Sandstone|67402|5|Briefly described|p90, p90 fig CPR4|||Deposited by high energy braided fluvial system and associated outwash fan deposits. See also p91 tbl CPR1, p99 fig CPR14, p101, p101 tbl CPR2, p104.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.|Fine-grained to pebbly, massive to planar cross-bedded sandstone with common beds of conglomerate, carbonaceous siltstone, shale and coal.|
18232|Tirrawarra Sandstone|68731|5|Briefly described|p200 Fig 3.110, p204, p205, p206|Cisuralian||(Kapel 1972; Gatehouse 1972). ~ 40 m thick. Deposited by melt-water streams flowing north from retreating glaciers as reworked unconsolidated glacial sediments and has yielded Cisuralian palynofloras.||Of the Gidgealpa Group.||Interdigitated with the Merrimelia Formation. Overlain by the Patchawarra Formation. Conformably underlain by the Merrimelia Formation.|Comprises fine to coarse and pebbly sandstone, with common conglomerates and minor carbonaceous siltstone, shale, and coal. Sandstone is massive, with flat or planar cross-bedding and a siliceous or kaolinitic matrix.|12-MAY-16
18232|Tirrawarra Sandstone|69023|4|Described|p79, p81, p82 Fig.18, p83, p191-192|Permian|Late Carboniferous|Cooper Basin. A more recent addition to the Gidgealpa Group: was recognised by Kapel (1972) and Gatehouse (1972). Gas reserves. Fluvio-glacial. Incorrectly labelled as Tirrawarra Formation on the CALLABONNA map reference. 54.9 to 69.5m thick. Stratigraphic wells intersection data.||Unit in Gidgealpa Group.||Overlies and interbedded with  Merrimelia Formation. Is overlain by Patchawarra Formation.|Buff-white to brownish, medium- to coarse-grained sandstone; massive to flat-bedded and cross-bedded, with a siliceous or kaolinitic matrix; rare pebbly sandstone to conglomerate; scarce carbonaceous mudstone and coal stringers.|
18232|Tirrawarra Sandstone|69454|4|Described|p38:3-4, 6-7, 12-13, 14 Fig.38.9|Sakmarian|Asselian|McKellar (2002). Defined in the Cooper Basin in SA and Qld. Rocks in the Pedirka Basin are referred to as 'Tirrawarra Sandstone equivalent', and were included as upper Crown Point Formation by Jones et al. (2011). 200m thick in Mount Hammersley-1. Glaciofluvial braided river/glacial outwash deposits. Has fair to good reservoir potential, sealed by basal Purni Formation shale (in the Pedirka Basin) or Patchawarra Formation (in the Cooper Basin).||||Conformably overlies and interfingers with Crown Point Formation. Is overlain conformably by Purni Formation.|Very fine to very coarse to conglomeratic feldspathic sandstone; minor siltstone and claystone.|22-AUG-18
18232|Tirrawarra Sandstone|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
18232|Tirrawarra Sandstone|69673|6|Mentioned|p149, p150, p151, p160|||||||Overlain by Purni Formation|Sandstone, conglomerate and lesser siltstone.|
18232|Tirrawarra Sandstone|69797|5|Briefly described|p17 Fig.2|Early Permian|Late Carbonfierous|Age: Stephanian - Asselian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
18232|Tirrawarra Sandstone|69946|5|Briefly described|p3, p9, p36, p45, p54|Sakmarian|Asselian|Southern Cooper Basin. Braided fluvial to proglacial outwash deposits.||||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation. Equivalent to Boorthanna Formation (Arckaringa Basin).||
18232|Tirrawarra Sandstone|69947|5|Briefly described|p13 Fig.7.2|Permian|Late Carboniferous|Cooper Basin.||Gidgealpa Group.||||
18232|Tirrawarra Sandstone|69982|5|Briefly described|p13, p44, Appendix 1|Permian|Permian|Cooper Basin. Hydrocarbon shows from the Warburton Basin rocks have been incorrectly assigned to this unit (and others). Brief thin section descriptions. Appears as "Tirrawarra sandstone" on p103.||||||
18232|Tirrawarra Sandstone|70317|6|Mentioned|p33, 36|Early Permian|Late Carboniferous|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Overlies Merrimelia Formation, locally unconformably. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|70823|4|Described|iv, p25-p27, p36, 51-53|Asselian|Pennsylvanian|Cooper Basin. Up to 75m thick. Deposited in a proglacial outwash or braided fluvial environment. Some debate about age. Palynofloras are consistent with APP1.21, 1.22 and basal APP21.palynological zones. Hosts a commercial oil reservoir that is briefly discussed. See also p40-p41, p78-p80, p82.||Gidgealpa Group||Overlies and interfingers with the Merrimelia Formation. Overlain by and interfingers with the Patchawarra Formation.|Fine to coarse-grained, moderately well sorted sandstone, common conglomerates with minor shale interbeds and rare thin coal seams and stringers.|22-AUG-18
18232|Tirrawarra Sandstone|70824|4|Described|p7-p9, p38, p43-p47, p122|Asselian|Gzhelian|Cooper Basin. Up to 75m thick. Deposited as proglacial outwash or in a braided fluvial environment. Outcrop and areal extent briefly discussed.||||Conformably overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.|Fine to coarse-grained, moderately well sorted sandstone, common conglomerates with minor shale interbeds and rare thin coal seams and stringers.|
18232|Tirrawarra Sandstone|70946|5|Briefly described|p1089|Permian|Carboniferous|Cooper Basin. Deposited in a proglacial outwash or braided fluvial environment.||Gidgealpa Group.||||08-OCT-18
18232|Tirrawarra Sandstone|71265|5|Briefly described|p589|Asselian|Asselian|Cooper Basin.||Gidgealpa Group.||Overlies Merrimelia Formation. Is overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|71342|5|Briefly described|Ch5 p3, Ch5 p9, Ch5 p36, Ch5 p45|Sakmarian|Asselian|Cooper Basin. Deposited in a braided fluvial to proglacial outwash environment. Palynological zone is given in fig 5.3 Ch5 p36. Thermal history briefly described in Ch9. See also Ch5 p54, Ch7 p13, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p7, Ch10 p13-p14, Ch10 p17, Ch10 p19-p20, Ch11 p8, Ch13 p9.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.||
18232|Tirrawarra Sandstone|71701|5|Briefly described|p155|Asselian|Gzhelian|Cooper Basin.||Gidgealpa Group||Overlies the Merrimelia Formation. Overlain by the Patchawarra Formation.||
18232|Tirrawarra Sandstone|72297|5|Briefly described|p742|||Cooper Basin. Contains minor oil reserves at Pepita, and has some reservoir potential. [Next paragraph]: The largest onshore Permian oilfield in Australia is reservoired in the Tirrawarra Sandstone.||||||
18232|Tirrawarra Sandstone|72497|5|Briefly described|p13, p17 Fig.11.|Early Permian|Late Carboniferous|Cooper Basin. Described as fluvioglacial outwash deposits and overlying braided stream environment .||||Overlies Merrimelia Formation with diachronous contact?||
18232|Tirrawarra Sandstone|73251|6|Mentioned|p62|Cisuralian|Late Carboniferous|Cooper Basin. Proglacial outwash and braided fluvial depositional environments. Contains[?] gas and oil.||Gidgealpa Group||Underlain by Merrimelia Formation. Overlain by Patchawarra Formation.||
18232|Tirrawarra Sandstone|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18232|Tirrawarra Sandstone|73495|5|Briefly described|p497, p499, p503-504, p506|||Cooper Basin. Top contact may represent an unconformity. Reflects a braided fluvioglacial to fluvial setting with floodplains and rare mires.||||Underlain by and interfingering with Merrimelia Formation. Overlain by the Patchawarra Formation.|Locally developed conglomerate beds, fine- to coarse-grained and moderately to well-sorted sandstones (sublitharenites), minor shales and rare, thin coal beds.|
18239|Tirroan Basalt|42895|5|Briefly described|p83|||||||||
18239|Tirroan Basalt|68421|5|Briefly described|Map Legend|Pliocene|Miocene|Bundaberg Volcanic Province.|||||Dark grey to black, fine-grained to glassy olivine basalt, basanite; some basal clastogenetic lava and yellow-brown streaky glass with black glass bands.|
18248|Tivoli Formation|13516|5|Briefly described|p159 fig 8, p164|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Brassal Subgroup|Includes Cooneana Sandstone Member|||
18248|Tivoli Formation|24082|5|Briefly described|p453|Late Triassic|Late Triassic|Of the Brassall Sub-Group.  Max. thickness: 480m.  Geological Province: Ipswich Basin.||||||
18248|Tivoli Formation|30087|4|Described|p3|||See also P3. Unit of Ipswich Coal Measures.||||||
18248|Tivoli Formation|30302|6|Mentioned|p414|||Refers to Allen and Staines(1959). See also P415||||||
18248|Tivoli Formation|30459|6|Mentioned|p309|||||||||
18248|Tivoli Formation|30465|6|Mentioned|p3|||See also P4-22||||||
18248|Tivoli Formation|30466|6|Mentioned|p4|||||||||
18248|Tivoli Formation|30467|6|Mentioned|p412|||||||||
18248|Tivoli Formation|30470|6|Mentioned|p458|||||||||
18248|Tivoli Formation|30517|6|Mentioned|p436|||||||||
18248|Tivoli Formation|31118|6|Mentioned|Table 1|||||||||
18248|Tivoli Formation|31756|6|Mentioned|p16|||||||||
18248|Tivoli Formation|32136|6|Mentioned|p5|||Miospores||||||
18248|Tivoli Formation|32180|5|Briefly described|p6|||||||||
18248|Tivoli Formation|33381|4|Described|p110|||Triassic. See also PP112-117 & 122||||||
18248|Tivoli Formation|34070|6|Mentioned|p2|||Triassic.  See also PP3,6,9,11||||||
18248|Tivoli Formation|35053|5|Briefly described|p35|||||||||
18248|Tivoli Formation|36172|6|Mentioned|Appendix|||||||||
18248|Tivoli Formation|36237|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
18248|Tivoli Formation|36243|6|Mentioned|Table 10A|||||||||
18248|Tivoli Formation|36351|6|Mentioned|p373|||||||||
18248|Tivoli Formation|36354|3|Fully described|p368|||||||||
18248|Tivoli Formation|36779|6|Mentioned|p7|||||||||
18248|Tivoli Formation|36941|6|Mentioned|p162|||||||||
18248|Tivoli Formation|37110|6|Mentioned|p288|||||||||
18248|Tivoli Formation|37111|4|Described|p292|||||||||
18248|Tivoli Formation|37755|6|Mentioned|p80|||See also P84.||||||
18248|Tivoli Formation|38074|5|Briefly described|Table 1|||||||||
18248|Tivoli Formation|38076|6|Mentioned|Table 3|||||||||
18248|Tivoli Formation|38306|6|Mentioned|p512|||||||||
18248|Tivoli Formation|38307|4|Described|p520|||||||||
18248|Tivoli Formation|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
18248|Tivoli Formation|39445|5|Briefly described|Table 9|||||||||
18248|Tivoli Formation|39943|6|Mentioned|Table 12A|||||||||
18248|Tivoli Formation|40623|5|Briefly described|p30|||See also P107||||||
18248|Tivoli Formation|41906|3|Fully described|Table 2 P17|||||||||
18248|Tivoli Formation|42187|6|Mentioned|p319|||||||||
18248|Tivoli Formation|42336|5|Briefly described|p4|||||||||
18248|Tivoli Formation|42405|6|Mentioned|Table 3 P.7|||||||||
18248|Tivoli Formation|42648|5|Briefly described|p41|||Brassal Subgroup||||||
18248|Tivoli Formation|42893|6|Mentioned|p8|||||||||
18248|Tivoli Formation|43910|14|Not recorded|p12,19|||||||||
18248|Tivoli Formation|43922|14|Not recorded|p325,326|||||||||
18248|Tivoli Formation|43984|14|Not recorded|p129,130|||||||||
18248|Tivoli Formation|43995|14|Not recorded|Tb.p10||Triassic|Part of Illawarra Coal Measures [??but Tivoli Fm in Qld & Illawarra Coal Measures in Sydney Basin, NSW CEBMarch98]||||||
18248|Tivoli Formation|44030|14|Not recorded|p125|||Possibly equivalent to Tingalpa Formation.||||||
18248|Tivoli Formation|44091|14|Not recorded|p51||Triassic|||||||
18248|Tivoli Formation|44510|2|Defined|p252-256,262,Figs.35|||Fig.36. Conformably overlies Cribb Conglomerate. Overlain conformably by Cooneana Formation.||||||
18248|Tivoli Formation|44542|2|Defined|p32,35,36||Middle Triassic|=Tivoli Stage..||||||
18248|Tivoli Formation|44687|6|Mentioned|p222|Late Triassic|Middle Triassic|Of Staines (1959). ?Equivalent of Tingalpa Formation.||||||21-MAR-13
18248|Tivoli Formation|44703|14|Not recorded|unknown (6 sheets)|||Not listed on white card. (Tivoli-Cooneana Formation)||||||
18248|Tivoli Formation|44708|14|Not recorded|unknown (183pp)|||Not listed on white card. (Tivoli-Cooneana Formation)||||||
18248|Tivoli Formation|44734|14|Not recorded|p5,7,17-19|||Pine Mountain area.||||||
18248|Tivoli Formation|44772|14|Not recorded|p1,3,5|||Formation of Ipswich Coal Measures.||||||
18248|Tivoli Formation|44775|4|Described|p7,8,map2||Triassic|||||||
18248|Tivoli Formation|44783|14|Not recorded|p13,16,18|||||||||
18248|Tivoli Formation|67402|5|Briefly described|p165 tbl LPB1, p223, p225|Carnian|Carnian|Ipswich Basin. Deposited in a lacustrine environment.||Brassall Subgroup||Overlies the Cribb Conglomerate. Overlain by the Blackstone Formation.|Sandstone, siltstone, conglomerates, mudstone and minor claystone associated with coal.|
18248|Tivoli Formation|68679|4|Described|p394-396|Late Triassic|Late Triassic|Ipswich Basin. Up to 500m thick. River channel (mainly), peat swamp and flood plain deposits in a meandering stream system. One of the two major coal producers in the Ipswich Coalfield.||Brassall Subgroup.|Cooneana Sandstone Member.|Conformably overlies the Kholo Subgroup. Equivalent to Tingalpa Formation.|Shale and coal, with minor sandstone and conglomerate lenses; at least 21 coal seams, of which 16 are stratigraphically and/or laterally significant. Coal seams are commonly split, and contain high amounts of interbedded clastic sediments.|
18248|Tivoli Formation|72297|5|Briefly described|p698, p751|Triassic|Triassic|Ipswich Basin. In ARM Swanbank 2 well, 28m of coal with high gas content was intersected and CSG was reported.||Ipswich Coal Measures.|Cochrane, Garden, Tantivy, Fiery, Waterstown, Tivoli, Eclipse and Bentley seams.|||
18254|Toby Barty Sandstone Member|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Of the Marimo Slate (Mary Kathleen Group). Sandstone, quartzite.||||||
18254|Toby Barty Sandstone Member|22461|5|Briefly described|Fig 2 p466|||Parent: Marimo Slate||||||
18254|Toby Barty Sandstone Member|30527|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18254|Toby Barty Sandstone Member|30531|2|Defined|p21|Precambrian|Precambrian|||||||
18254|Toby Barty Sandstone Member|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18254|Toby Barty Sandstone Member|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18254|Toby Barty Sandstone Member|39496|4|Described|p13|||||||||
18254|Toby Barty Sandstone Member|41791|6|Mentioned|p255|||||||||
18254|Toby Barty Sandstone Member|45161|5|Briefly described|p50|||||||||
18254|Toby Barty Sandstone Member|45166|5|Briefly described|p24|||||||||
18254|Toby Barty Sandstone Member|49009|6|Mentioned|p45|||||||||
18254|Toby Barty Sandstone Member|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Feldspathic arenite and quartzite.||||||
18263|Toko Group|10116|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Includes: Nora Formation, Carlo Sandstone, Mithaka Formation, Ethabuka Sandstone.||||||
18263|Toko Group|13995|6|Mentioned|p77|||Georgina Basin.||||||
18263|Toko Group|24065|4|Described|p235|Middle Ordovician|Early Ordovician|Geological Province: Georgina Basin.||||||
18263|Toko Group|30914|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
18263|Toko Group|31714|6|Mentioned|Fig. 4|||||||||
18263|Toko Group|33111|6|Mentioned|p17|||||||||
18263|Toko Group|33738|6|Mentioned|p54|||||||||
18263|Toko Group|34252|6|Mentioned|Po.2|||Fossils||||||
18263|Toko Group|34454|5|Briefly described|Table 2|||Ordovician||||||
18263|Toko Group|35121|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
18263|Toko Group|35139|6|Mentioned|p16|||||||||
18263|Toko Group|35146|6|Mentioned|p468|||||||||
18263|Toko Group|36234|6|Mentioned|Fig.1|||||||||
18263|Toko Group|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
18263|Toko Group|36580|1|Redefined|p473|Middle Ordovician|Early Ordovician|Early to Middle Ordovician. See also Fig.1||||||
18263|Toko Group|37572|6|Mentioned|p164|||||||||
18263|Toko Group|37727|6|Mentioned|Fig.1|||||||||
18263|Toko Group|37735|6|Mentioned|p12|||Assigned to the wrong state.||||||
18263|Toko Group|38832|6|Mentioned|p157|||||||||
18263|Toko Group|39445|6|Mentioned|p61|||See also p64, Table 4 and Fig.5.||||||11-DEC-06
18263|Toko Group|40136|5|Briefly described|p41|||||||||
18263|Toko Group|43808|6|Mentioned|p293|||||||||
18263|Toko Group|44091|14|Not recorded|p19,Tb.1||Early Ordovician|||||||
18263|Toko Group|44211|14|Not recorded|p95-99,103|Llanvirnian|Arenigian|Rests unconformably on Ninmaroo Formation. (Arenigian and perhaps Llanvirian or younger)||||||
18263|Toko Group|44233|14|Not recorded|Fig.1||Ordovician|Lower-Middle Ordovician.||||||
18263|Toko Group|44308|14|Not recorded|p10||Ordovician|||||||
18263|Toko Group|44309|14|Not recorded|Tb.1,p11,12,map|||Consists of Nora Formation, Carlo Sandstone, Mithaka Formation, Coolibah Formation.||||||
18263|Toko Group|44310|14|Not recorded|Map Legend|||Not listed on white card.||||||
18263|Toko Group|44312|14|Not recorded|Map Legend||Early Ordovician|(Middle Ordovician)||||||
18263|Toko Group|44326|14|Not recorded|Map Legend|Early Ordovician|Early Ordovician|(Early-Middle Ordovician)||||||
18263|Toko Group|44358|3|Fully described|App.p19|Early Ordovician|Early Ordovician|See also p9-10, (Early-Middle Ordovician)||||||
18263|Toko Group|44469|14|Not recorded|p.10|||(F53-12).||||||
18263|Toko Group|44470|5|Briefly described|map legend|||||||||02-DEC-04
18263|Toko Group|44543|14|Not recorded|p34|||Ref. to Queensland Geological Map 1953. See also Lexicon.||||||
18263|Toko Group|44920|14|Not recorded|Map Legend, Sheet 4||Ordovician|Ordovician||||||
18263|Toko Group|45052|4|Described|p126|||Constituent formations||||||
18263|Toko Group|45118|6|Mentioned|p4|||||||||
18263|Toko Group|46940|6|Mentioned|p57|||||||||
18263|Toko Group|46973|6|Mentioned|p53|||||||||
18263|Toko Group|48901|14|Not recorded|Not recorded|||||||||
18263|Toko Group|48906|14|Not recorded|Tb.1|||||||||
18263|Toko Group|49027|6|Mentioned|p17|||||||||
18263|Toko Group|60122|5|Briefly described|p5, p29-30|Early Ordovician|Early Ordovician|Originated as Toko Series (Whitehouse 1936). Historically the group has included, then excluded, and now includes Kelly Creek Fm. Similarly Coolibah Fm. has been included, excluded and now remains included. Also Includes Nora Fm, Carlo Sst and Mithaka Fm.||||||24-MAY-05
18263|Toko Group|60590|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Includes the Coolibah, Nora and Mithaka Formations and Carlo Sandstone.||||||26-NOV-04
18263|Toko Group|61404|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Comprises: Kelly Creek, Coolobah, Nora Formations, Carlo Sandstone, Mithaka Formation and Ethabuka Sandstone. Geological Province: southern Georgina Basin.||||||
18263|Toko Group|62983|5|Briefly described|p11|Middle Ordovician|Early Ordovician|Marine siliciclastic sedimentation. Thickness: 370m. Geological Province: Georgina Basin.||||||
18263|Toko Group|63562|6|Mentioned|p349|Early Ordovician|Late Cambrian|Of Georgina Basin.|||||Carbonates and siliciclastics.|
18263|Toko Group|64068|1|Redefined|p226, pp75-78, p7, 38, p ix|Late Ordovician|Late Cambrian|Intended as a redefinition. Southern Georgina Basin.|||Includes Kelly Creek, Coolibah, Nora and Mithaka Formations, Carlo and Ethabuka Sandstones.|Overlies Tomahawk and Ninmaroo Formations. Is overlain unconformably by Dulcie Sandstone and Cravens Peak beds.|Marine siliciclastics.|22-MAR-16
18263|Toko Group|66767|5|Briefly described|p59|Late Ordovician|Early Ordovician|Southern Georgina Basin.|||Kelly Creek Formation.||Marine siliciclastic sedimentary rocks including dolomitic quartz sandstone and dolostone.|
18263|Toko Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.||||||Includes Carlo Sandstone, Coolibah Formation, Ethabuka Sandstone, Kelly Creek Formation, Mithaka Formation, Nora Formation|||
18263|Toko Group|67870|5|Briefly described|p43, p46-47, p50-53|Ordovician|Ordovician|Georgina Basin. Potential hydrocarbon reservoir.|||||Sandstone, shale, limestone (chalk), siltstone, glauconite.|
18263|Toko Group|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Georgina Basin. This unit, as well as Kelly Creek and Coolibah Formations, are all mapped under the symbol, Ot.||||||
18263|Toko Group|69443|4|Described|p28:3-4, 7, 26-31|Late Ordovician|Early Ordovician|Casey in Smith (1963), after Whitehouse (1936). Southern Georgina Basin. Forms scarps, plateaux and hills. Combined maximum thickness of 1678m. Is correlated with Hanson River beds (Wiso Basin), Florina Formation (Daly Basin), the poorly dated Djagamara Formation and Kerridy Sandstone (Ngalia Basin), and Pacoota Sandstone, Horn Valley Siltstone, Stairway Sandstone, Stokes Siltstone and Carmichael Sandstone (Amadeus Basin).|||Kelly Creek, Coolibah, Nora, Mithaka Formations; Carlo, Ethabuka Sandstones.|Overlies Cockroach Group conformably to locally disconformably, or Georgina Limestone unconformably. Is overlain unconformably by Cravens Peak beds.||12-JUL-16
18263|Toko Group|69591|4|Described|p95, p112|Late Ordovician|Middle Ordovician|Crops out in the Toko Syncline which straddles the QLD/NT border. Originally the Toko Series of Whitehouse (1936), which included the upper part of the Nora Formation and the Carlo Sandstone. Casey (cited in Smith, 1963) applied the name Toko Group to Kelly Creek, Coolibah, Nora, Mithaka Formations and Carlo Sandstone, then revised it by removing Kelly Creek Formation (cited in Smith, 1965). Draper (1980) added the newly named Ethabuka Sandstone and removed the Coolibah Formation: this is the formulation used in this study. Webby et al. (1981) rejected this and included the Coolibah Formation and excluded the Ethabuka Sandstone. Kruse et al. (2002) and Kruse and Mohammed (2005) followed Casey (cited in Smith, 1963), including Kelly Creek and Coolibah Formations and Ethabuka Sandstone.|||Nora, Mithaka Formations; Carlo, Ethabuka Sandstones.||Clastic sediments, dominantly sandstone.|
18263|Toko Group|69673|6|Mentioned|p111, p114 fig 92, p118, p119 fig 94|Ordovician|Ordovician||||Includes Kelly Creek Formation, Coolibah Formation, Nora Formation, Carlo Sandstone, Mithaka Formation, Ethabuka Sandstone|||
18309|Tomato Granite|22847|3|Fully described|p 41|||||||||
18309|Tomato Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
18309|Tomato Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 84. I-Type.||||||
18309|Tomato Granite|42245|2|Defined|p32|Ordovician||Reserved as Tomato Adamellite||||||
18309|Tomato Granite|43093|4|Described|Appendix 1||Ordovician|||||||
18309|Tomato Granite|43259|4|Described|Appendix 1,p21.||Ordovician|||||||
18309|Tomato Granite|43935|5|Briefly described|Map Legend||Ordovician|||||||
18352|Toogoolawah Group|13516|5|Briefly described|p159 fig 8|Middle Triassic|Middle Triassic|From Clarence-Moreton Basin, Ipswich Basin.|||Includes Esk Formation, Neara Volcanics, Bryden Formation.|||
18352|Toogoolawah Group|22857|5|Briefly described|p277|Middle Triassic|Middle Triassic|Intermediate to felsic calc-alkaline volcanics and volcaniclastic sediments. Max. thickness: >5km. Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|22860|5|Briefly described|p277||Middle Triassic|||||||
18352|Toogoolawah Group|23440|4|Described|p140|Triassic|Triassic|||||||
18352|Toogoolawah Group|23800|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|24279|5|Briefly described|p1800|Middle Triassic.|Early Triassic|Terrestrial sedimentary and volcanic rocks. Overlain by Aranbanga Volcanic Group.||||||
18352|Toogoolawah Group|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|Constituents include: Kinellan Basalt, Gayndah Formation and Mount Marcella Volcanics||||||
18352|Toogoolawah Group|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|29386|5|Briefly described|p454|||Lower - Middle Triassic.||||||
18352|Toogoolawah Group|30302|6|Mentioned|p414|||Lower - Middle Triassic age||||||
18352|Toogoolawah Group|30303|6|Mentioned|p322|||Lower(?)to Middle Triassic. Strat.relationships with Cressbrook Group.||||||
18352|Toogoolawah Group|30470|6|Mentioned|p458|||||||||
18352|Toogoolawah Group|30473|6|Mentioned|p377|||Refers Granfield & Schawarzbock (1972)||||||
18352|Toogoolawah Group|30508|6|Mentioned|p91|||Triassic age. Palynology||||||
18352|Toogoolawah Group|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
18352|Toogoolawah Group|31118|6|Mentioned|p323|||Possible oil source||||||
18352|Toogoolawah Group|31450|6|Mentioned|p47|||||||||
18352|Toogoolawah Group|31811|6|Mentioned|p27|||||||||
18352|Toogoolawah Group|33774|6|Mentioned|p42|||Lower Middle Triassic. Refers Cranfield & Schwarzbock (1972)||||||
18352|Toogoolawah Group|33881|5|Briefly described|p96|||||||||
18352|Toogoolawah Group|35101|3|Fully described|p35|||||||||
18352|Toogoolawah Group|35161|6|Mentioned|p591|||||||||
18352|Toogoolawah Group|35428|6|Mentioned|p125|||Biostratigraphy||||||
18352|Toogoolawah Group|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
18352|Toogoolawah Group|36045|6|Mentioned|p334|||||||||
18352|Toogoolawah Group|36243|6|Mentioned|p74|||See also Table 10A.||||||
18352|Toogoolawah Group|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
18352|Toogoolawah Group|36954|6|Mentioned|p114|||||||||
18352|Toogoolawah Group|36961|6|Mentioned|Table 1|||||||||
18352|Toogoolawah Group|37065|6|Mentioned|p36|||||||||
18352|Toogoolawah Group|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
18352|Toogoolawah Group|37755|6|Mentioned|p79|||||||||
18352|Toogoolawah Group|38304|6|Mentioned|p83|||||||||
18352|Toogoolawah Group|38391|6|Mentioned|p10|||||||||
18352|Toogoolawah Group|38441|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
18352|Toogoolawah Group|39079|6|Mentioned|p10|||||||||
18352|Toogoolawah Group|39445|6|Mentioned|Table 9|||||||||
18352|Toogoolawah Group|39943|6|Mentioned|Table 12A|||||||||
18352|Toogoolawah Group|40051|6|Mentioned|p8|||||||||
18352|Toogoolawah Group|40245|6|Mentioned|p182|||See also Table 2.||||||
18352|Toogoolawah Group|40475|5|Briefly described|p7|||||||||
18352|Toogoolawah Group|40480|6|Mentioned|p40|||||||||
18352|Toogoolawah Group|40623|5|Briefly described|p66|||||||||
18352|Toogoolawah Group|41591|5|Briefly described|p17|||||||||
18352|Toogoolawah Group|41736|6|Mentioned|p115|||||||||
18352|Toogoolawah Group|41738|4|Described|p165|||||||||
18352|Toogoolawah Group|41778|6|Mentioned|Fig.1|||||||||
18352|Toogoolawah Group|41790|5|Briefly described|p471|||||||||
18352|Toogoolawah Group|41906|3|Fully described|Table 2 P19|||||||||
18352|Toogoolawah Group|41917|6|Mentioned|Fig.3 P528|||||||||
18352|Toogoolawah Group|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Includes: Esk and Bryden Formations and the Neara Volcanics.||||||15-JUL-04
18352|Toogoolawah Group|42893|6|Mentioned|p6|||||||||
18352|Toogoolawah Group|43001|6|Mentioned|p120|||||||||
18352|Toogoolawah Group|43002|5|Briefly described|Fig.2,p135|||||||||
18352|Toogoolawah Group|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Includes: Esk Formation, Neara Volcanics, Bryden Formation.||||||
18352|Toogoolawah Group|60281|5|Briefly described|p24|Middle Triassic|Early Triassic|Geological Province: Esk Trough.||||||20-JAN-05
18352|Toogoolawah Group|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Includes the Bryden Formation, Neara Volcanics and Esk Formation.||||||
18352|Toogoolawah Group|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Includes the Gayndah Formation, Esk Formation and Neara Volcanics. Geological Province: Esk Trough||||||02-SEP-04
18352|Toogoolawah Group|61002|5|Briefly described|p198 Fig 2|Middle Triassic|Middle Triassic|Nonmarine polymict and volcaniclastic conglomerate, sandstone and shale with interbedded andesitic lava and tuff. Max. thickness: 2350m. Geological Province: Esk Trough. See also p199, p202.||||||29-MAY-06
18352|Toogoolawah Group|61005|5|Briefly described|p248|Middle Triassic|Middle triassic|Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|61310|6|Mentioned|p25|||||||||
18352|Toogoolawah Group|61781|6|Mentioned|p267|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|61782|4|Described|p275|Middle Triassic|Early Triassic|Includes; Gayndah Formation, Mount Marcella Volcanics and Kinellan Basalt. Unconfomably overlie Marumba Beds, nonconformity with Claddagh Granodiorite. Max thick: 6000m. Geol Prov: Esk Trough.||||||
18352|Toogoolawah Group|63821|4|Described|p12, p19-20|Middle Triassic|Early Triassic|Comprises Kinella Basalt (base), Gayndah Formation, Mount Marcella Volcanics (top). Unconformably overlain by Aranbanga Volcanic Group. Geological Province: Esk Trough. Series of volcanic flows, pyroclastics, volcaniclastic sediments and fluvial deposits.||||||07-FEB-11
18352|Toogoolawah Group|64197|6|Mentioned|p630 Fig.7|Triassic|Triassic|Moreton Basin/Esk Trough.||||||
18352|Toogoolawah Group|65452|5|Briefly described|p37|Middle Triassic|Early Triassic|Gayndah area. Thought to represent subduction-related magmatism.|||Mount Marcella Volcanics.|||
18352|Toogoolawah Group|67402|5|Briefly described|p204, p207, p208|Ladinian|Anisian|Esk Trough.|||Includes the Esk Formation, Bryden Formation and the Neara Volcanics||Conglomerates, sandstone, shale and volcanics.|
18352|Toogoolawah Group|67874|6|Mentioned|p11||||||Includes Mount Marcella Volcanics.|||06-NOV-15
18352|Toogoolawah Group|68008|5|Briefly described|p188|Triassic|Triassic|Fills the Esk Trough,||||Correlated with Cynthia beds.||
18352|Toogoolawah Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Muncon Volcanics and Native Cat Andesite, are all mapped under the symbol, Rvm.||||||
18352|Toogoolawah Group|68679|5|Briefly described|p312-313, p371, p385, p387-392,p420,p439|Middle Triassic|Early Triassic|The surface exposure of this unit defines the extent of the Esk Basin, northern New England Orogen. Includes units previously part of the Esk Series. Differing interpretations of the Basin's stratigraphy are outlined, and different unit names are applied in the northern part of the Basin. The former Mount Marcella Volcanics are mostly regarded as a northern equivalent to the Neara Volcanics. Estimates of thickness range from 2350m to 5000-6000m. Entirely continental deposits. Contains Middle Triassic macrofloras similar to those in the Brooweena Formation (Gympie Province). Basin evolution discussed.|||Bryden, Esk Formations and Neara Volcanics (southern Esk Basin); Kinellan Basalt, Gayndah Formation (northern Esk Basin).|Is faulted against and unconformably overlies the Cressbrook Creek Group, Northbrook beds and Marumba beds. Overlies Chowey and Mingo Granites. Is overlain unconformably by Abernethy Basalt.||
18352|Toogoolawah Group|69594|5|Briefly described|p560-561|Triassic|Triassic|W and NW of Brisbane.||||Is intruded by the Brisbane Valley Porphyrites.||
18352|Toogoolawah Group|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.|||Bryden, Esk Formations; Neara Volcanics.|Correlated with Moolayember Formation.|Continental volcaniclastic conglomerate, sandstone, shale, and intermediate volcanic rocks.|
18352|Toogoolawah Group|73450|6|Mentioned|p107|Triassic|Triassic|||||||
18357|Toolachee Formation|13497|3|Fully described|iv, v, vi, viii, x, xi|Late Permian|Late Permian|Cooper Basin. Named by Kapel (1972) and defined by Gatehouse (1972). Morton and Gatehouse (1985) redefined the formation to exclude parts of the Daralingie Formation included in the type section. A type section is briefly mentioned. Petrography and fossil assemblage is discussed in some detail.  A sedimentary facies log is provided on p102 including detailed descriptions of its lithology and depositional environments. Coal and carbonaceous shale of this unit are the second most important source rocks in the Cooper Basin. Coal thickness exceeds 35m in the Patchawarra Trough and 25m in the Weena Trough. Reservoir characteristics discussed.  Unconformably overlies the Daralingie Formatio, Epsilon Formation and the Murteree Shale. Overlain conformably by the Arrabury Formation (Nappamerri Group). See also xii, p50, p58, p63-p67, p69 fig 6.1, p70-p73, p89, p93, p96, p99, p101-p105, p119, p122, p125, p127, p129, p131, p132 tbl 8.1-8.2, p133, p138 fig 8.17, p139 fig 8.18, p141, p144 fig 9.2, p146, p148-p153, p157, p159-p162, p164-p165, p168, p170-p171, p173-p176, p182-p183, p187, p191-p193, p195, p204-p205, p216.||Gidgealpa Group||Disconformably overlies the Patchawarra Formation.|Interbedded buff to white, fine to coarse-grained sandstone, dark grey siltstone and dark grey to black carbonaceous shale that is sometimes sideritic with thin coal seams and conglomerates.|
18357|Toolachee Formation|13516|6|Mentioned|p147, fig 5, p155|Late Permian|Late Permian|From Cooper Basin||||||
18357|Toolachee Formation|22527|6|Mentioned|p 1|||||||||
18357|Toolachee Formation|22817|5|Briefly described|p28|Late Permian|Late Permian|||||||
18357|Toolachee Formation|22839|6|Mentioned|P33||Late Permian|||||||
18357|Toolachee Formation|22883|6|Mentioned|P29|||Overlying unit is Arrabury Formation||||||
18357|Toolachee Formation|22909|5|Briefly described|42|||||||||
18357|Toolachee Formation|22924|6|Mentioned|49|||||||||
18357|Toolachee Formation|23154|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province - Cooper Basin. Of the Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|23155|4|Described|p22|Late Permian|Late Permian|Age determined from palynological evidence.  The unit consitutes the top unit of the Gidgealpa Group.  Max thickness is about 152m in the Toolachee- Munkarie area.  On STRZELECKI the Toolachee Formation is overlain conformably by Arrabury Formation.||||||
18357|Toolachee Formation|23375|4|Described|Fig2 p265|Dzhulfian|Midian|In the Cooper Basin.||||||12-DEC-06
18357|Toolachee Formation|23832|4|Described|p330|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24199|5|Briefly described|p512|Late Permian|Late Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24210|5|Briefly described|p133 Fig. 2|Late Permian|Late Permian|Of the Gidgealpa Group.  Geological Province: Cooper Basin.  See also p132.||||||
18357|Toolachee Formation|24212|6|Mentioned|p67, p69, p75|||Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|24240|5|Briefly described|p21|Permian|Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|29387|6|Mentioned|Table 2|||Refers to Gatehouse(1972).||||||
18357|Toolachee Formation|29389|6|Mentioned|p18|||Permian.||||||
18357|Toolachee Formation|29391|6|Mentioned|Table 5|||Appears on p23.||||||12-DEC-06
18357|Toolachee Formation|29513|6|Mentioned|p23|||||||||
18357|Toolachee Formation|29518|6|Mentioned|p24|||||||||
18357|Toolachee Formation|29520|6|Mentioned|p18|||||||||
18357|Toolachee Formation|29526|6|Mentioned|p18|||||||||
18357|Toolachee Formation|29721|6|Mentioned|p165|||||||||
18357|Toolachee Formation|29729|6|Mentioned|p266|||||||||
18357|Toolachee Formation|30515|6|Mentioned|p66|||See also p68. Part of Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|30519|5|Briefly described|p73|||Part of Gidgealpa Group. See also p75.||||||12-DEC-06
18357|Toolachee Formation|30540|6|Mentioned|p65|||General geology||||||
18357|Toolachee Formation|30543|6|Mentioned|p104|||||||||
18357|Toolachee Formation|30544|6|Mentioned|p53|||||||||
18357|Toolachee Formation|30825|6|Mentioned|p37|||||||||
18357|Toolachee Formation|30873|2|Defined|p13|Permian|Permian|Part of Gidgealpa Group.||||||12-DEC-06
18357|Toolachee Formation|30921|6|Mentioned|Map legend|Tatarian|Kungurian|Kungurian - Tatarian||||||
18357|Toolachee Formation|32696|6|Mentioned|Fig.4|||See also Figs. 6,7,8,9||||||
18357|Toolachee Formation|33074|6|Mentioned|p260|||||||||
18357|Toolachee Formation|33192|6|Mentioned|p18|||||||||
18357|Toolachee Formation|33331|6|Mentioned|p40|||||||||
18357|Toolachee Formation|33372|6|Mentioned|p25|||||||||
18357|Toolachee Formation|33489|3|Fully described|p42|||Structural and sedimentological development.||||||12-DEC-06
18357|Toolachee Formation|33976|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|34839|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|35067|6|Mentioned|Fig.4|||||||||
18357|Toolachee Formation|35068|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|35151|6|Mentioned|p147|||||||||
18357|Toolachee Formation|35279|6|Mentioned|p19|||||||||
18357|Toolachee Formation|35457|6|Mentioned|p629|||Also Fig.4 biostratigraphic relationships||||||
18357|Toolachee Formation|35573|6|Mentioned|Fig.7|||Generalised stratigraphy - Southern Cooper Basin||||||
18357|Toolachee Formation|35845|4|Described|p24|||Lithology and depositional environments. See also Fig.25.||||||17-JAN-08
18357|Toolachee Formation|36099|6|Mentioned|p191|||||||||
18357|Toolachee Formation|36331|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|36613|6|Mentioned|p1864|||||||||
18357|Toolachee Formation|36643|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|36910|6|Mentioned|p61|||||||||
18357|Toolachee Formation|36917|6|Mentioned|p143|||||||||
18357|Toolachee Formation|36924|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|37065|6|Mentioned|p32|||||||||
18357|Toolachee Formation|37103|5|Briefly described|p266|||||||||
18357|Toolachee Formation|37287|6|Mentioned|p36|||||||||
18357|Toolachee Formation|37565|6|Mentioned|Fig.8|||||||||
18357|Toolachee Formation|37703|6|Mentioned|p2240|||||||||
18357|Toolachee Formation|37855|6|Mentioned|p4|||||||||
18357|Toolachee Formation|37917|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|38730|6|Mentioned|p29|||||||||
18357|Toolachee Formation|38908|6|Mentioned|p8|||||||||
18357|Toolachee Formation|38958|5|Briefly described|p495|||||||||
18357|Toolachee Formation|38977|6|Mentioned|Fig.1|||||||||
18357|Toolachee Formation|39252|5|Briefly described|p20|||See also p26, p28 and Fig.15.||||||12-DEC-06
18357|Toolachee Formation|39254|5|Briefly described|p46|||See also p47.||||||12-DEC-06
18357|Toolachee Formation|39255|6|Mentioned|p51|||||||||
18357|Toolachee Formation|39261|6|Mentioned|Fig. 9|||||||||
18357|Toolachee Formation|39264|6|Mentioned|Fig. 13|||||||||
18357|Toolachee Formation|39276|6|Mentioned|p335|||oil & gas in Tartulla No.1||||||
18357|Toolachee Formation|39445|5|Briefly described|Table 8|||||||||
18357|Toolachee Formation|39478|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|39494|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|39757|6|Mentioned|p1601|||||||||
18357|Toolachee Formation|40030|6|Mentioned|Fig.3|||||||||
18357|Toolachee Formation|40056|1|Redefined|p11|Late Permian|Late Permian|||||||
18357|Toolachee Formation|40249|6|Mentioned|p45|||||||||
18357|Toolachee Formation|40544|6|Mentioned|p156|||||||||
18357|Toolachee Formation|40637|6|Mentioned|Fig.2|||||||||
18357|Toolachee Formation|41060|6|Mentioned|Fig.5|||||||||
18357|Toolachee Formation|41099|6|Mentioned|p185|||||||||
18357|Toolachee Formation|41123|6|Mentioned|p180|||||||||
18357|Toolachee Formation|41131|5|Briefly described|Table 1|||||||||
18357|Toolachee Formation|41164|6|Mentioned|p422|||||||||
18357|Toolachee Formation|41165|6|Mentioned|Fig.18|||||||||
18357|Toolachee Formation|41176|6|Mentioned|p206|||||||||
18357|Toolachee Formation|41183|6|Mentioned|Fig.3 p308|||||||||
18357|Toolachee Formation|41184|6|Mentioned|p348|||||||||
18357|Toolachee Formation|41189|6|Mentioned|p249|||||||||
18357|Toolachee Formation|41195|6|Mentioned|p325|||||||||
18357|Toolachee Formation|41198|6|Mentioned|p44|||||||||
18357|Toolachee Formation|41214|6|Mentioned|p256|||||||||
18357|Toolachee Formation|41223|6|Mentioned|p407|||||||||
18357|Toolachee Formation|41267|6|Mentioned|p256|||||||||
18357|Toolachee Formation|41288|6|Mentioned|p159|||||||||
18357|Toolachee Formation|41536|6|Mentioned|p373|||||||||
18357|Toolachee Formation|41595|6|Mentioned|p31|||||||||
18357|Toolachee Formation|41689|6|Mentioned|Table 1|||||||||
18357|Toolachee Formation|41707|6|Mentioned|Fig.8|||||||||
18357|Toolachee Formation|41712|6|Mentioned|p282|||See also P289||||||
18357|Toolachee Formation|42006|6|Mentioned|Fig.1 P21|||||||||
18357|Toolachee Formation|42008|6|Mentioned|p270|||||||||
18357|Toolachee Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18357|Toolachee Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18357|Toolachee Formation|42150|6|Mentioned|p65|||||||||
18357|Toolachee Formation|42187|6|Mentioned|Fig.2 P318|||||||||
18357|Toolachee Formation|42256|6|Mentioned|Fig.1 P243|||||||||
18357|Toolachee Formation|42395|6|Mentioned|p80|||||||||
18357|Toolachee Formation|42496|5|Briefly described|App.1 P152, Fig.3 P2|||||||||
18357|Toolachee Formation|42599|6|Mentioned|p624|||Cooper Basin.||||||
18357|Toolachee Formation|42648|5|Briefly described|p41, p48|||||||||
18357|Toolachee Formation|42746|5|Briefly described|p6|||||||||
18357|Toolachee Formation|42999|5|Briefly described|Table 2,p90||Late Permian|||||||
18357|Toolachee Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18357|Toolachee Formation|43105|5|Briefly described|Fig.7,p13|||||||||
18357|Toolachee Formation|43570|6|Mentioned|Fig.2,p535|Late Permian|Early Permian|(Kayanian-Tatarian)||||||
18357|Toolachee Formation|43628|6|Mentioned|Fig.3|Late Permian|Late Permian|||||||
18357|Toolachee Formation|44133|4|Described|p65 Fig. 8.3, 82, 85|Tatarian|Kazanian|Of the Gidgealpa Group. Geological Province: Cooper Basin. Conformably overlain by the Arrabury Formation (Nappamerri Group). Maximum Thickness: 160m.||||||17-JAN-08
18357|Toolachee Formation|46849|6|Mentioned|p191|||||||||
18357|Toolachee Formation|48995|6|Mentioned|p50|||See also P50.||||||
18357|Toolachee Formation|60386|6|Mentioned|p296|Lopingian|Guadalupian|Cooper Basin. Non-marine. Age shown as Ufimian to Changhsingian.||||||
18357|Toolachee Formation|60717|5|Briefly described|p40|Middle Triassic|Late Permian|Of the Nappamerri Group. Overlain by Arrabury Formation. Thickness: 160m. Geological Province: Cooper Basin. See also Figure 2.||||||31-JAN-08
18357|Toolachee Formation|61613|6|Mentioned|p282 Fig. 2|Late Permian|Late Permian|Geological Province: Cooper and Simpson Basins.||||||07-FEB-11
18357|Toolachee Formation|61614|5|Briefly described|p289, p290, p290 Fig. 2|Late Permian|Late Permian|Of Gidgealpa Group. Geological Province: Cooper Basin. Contain coal and shale lithologies.||||||17-MAR-09
18357|Toolachee Formation|61615|5|Briefly described|p302, p303, p302 Fig. 2, p304, p307|Late Permian|Late Permian|Of Gidgealpa Group. Conformably overlain by Nappamerri Group. Geological Province: Cooper Basin. Deposited in a fluvial, peat swamps and lacustrine environments.||||||07-FEB-11
18357|Toolachee Formation|61616|6|Mentioned|p329|Permian|Permian|Of Gidgealpa Group. Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|61617|6|Mentioned|p343, p346|Permian|Permian|Geological Province: Cooper Basin.||||||
18357|Toolachee Formation|62046|5|Briefly described|p125 Fig. 2|Permian|Permian|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
18357|Toolachee Formation|62537|6|Mentioned|p191 Fig.2. |Late Permian|Late Permian|Cooper Basin.||Unit in Gidgealpa Group.||Is overlain by Callamurra Member of the Arrabury Formation.||
18357|Toolachee Formation|62730|5|Briefly described|p352 Fig. 1|Late Permian|Late Permian|Geological Province: Cooper Basin.||||||21-APR-08
18357|Toolachee Formation|63832|6|Mentioned|p131 fig 2|Lopingian|Guadalupian|Of Cooper Basin.||||||
18357|Toolachee Formation|63978|2|Defined|p17, Fig. 3|Late Permian|Middle Permian|Originally included upper Gidgealpa Gp. Disconformable on Daralingie Fm; also unconformable on Patchawarra Fm.in places; conformable below Arrabury Fm. Max. thick:190m. Interbedded sandst., siltstone, mudstone + shale?.detailed lith. incl. In Cooper Basin||||||27-NOV-15
18357|Toolachee Formation|64048|5|Briefly described|p63, p64 Tb. 2, p66|Late Permian|Permian|Max. thickness: >150m. Source of hydrocarbons - coal measures. Hosts largest gas reservoir in SA. Geological Province: Cooper Basin.||||||07-FEB-11
18357|Toolachee Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Permian|Late Permian|Cooper Basin.||||Underlies the Callamurra Member of the Nappamerri Group.||11-DEC-15
18357|Toolachee Formation|64631|5|Briefly described|p44 Fig.2.|Changhsingian|Wordian|Cooper Basin. Biostratigraphic age control for base and top.||||Is overlain by Nappamerri Group. Unconformably underlain by Daralingi Formation.||
18357|Toolachee Formation|64665|5|Briefly described|p53 Fig.2, p56.|Late Permian|Middle Permian|Cooper Basin. Hosts coal: equivalent to Betts Creek beds (Galilee Basin) and Bandanna Formation (Bowen Basin). Inertinite-rich, vitrinite-poor; medium volatile bituminous to anthracite. Located at uneconomic depths; source rock maturation has produced substantial oil and gas production.||||Is overlain by Arrabury Formation.||
18357|Toolachee Formation|65238|5|Briefly described|p9|Late Permian|Late Permian|Geological province: Cooper Basin. In sedimentary continuum with the overlying Arrabury Formation.||||||17-FEB-10
18357|Toolachee Formation|65489|5|Briefly described|p15, p45, p47-50, p73, p96, p131-132|Permian|Permian|Cooper Basin. 160m thick. Gas and oil reservoir accounting for 56% and 0.6% respectively of the Basin's production. Regarded as the richest source unit in the Cooper-Eromanga Basins. Mis-spelt as Toollachee on p48.||Unit in Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain conformably by Arrabury Formation (Nappamerri Group).|Includes multi-zone high-sinuosity fluvial sandstones.|
18357|Toolachee Formation|65925|5|Briefly described|Appendix 2.||||||||Sandstone; mudstone; coal. Mixed-load channels, flood-plain and swamp.|
18357|Toolachee Formation|67402|5|Briefly described|p43 tbl HPB1, p90-p94|||Cooper Basin. Highly prospective reservoir formation for the storage of carbon dioxide with a potential storage capacity of 43.2 Megatonnes. Deposited in a meandering fluvial environment. See also p96, p98, p99 fig CPR14, p100, p101, p101 tbl CPR2, p103-p105, p268, p303.||Gidgealpa Group||Unconformably overlies the Daralingie Formation. Conformably overlain by the Callamurra Member.|Fining upwards deposits of coarse-grained sandstone, coal, carbonaceous siltstone, mudstone and shale.|
18357|Toolachee Formation|68731|5|Briefly described|p200 Fig 3.110, p204, p206, p207|Lopingian|Guadalupian|Cooper Basin. Originally incorporated rocks now assigned to the Daralingie Formation. Detailed lithology discussed. ~ < 190 m thick. Contains late Capitanian(?)-Lopingian palynofloras. Disconformably underlain by the Daralingie Formation.||Of the Gidgealpa Group.|Includes the Munkarie beds (basal unit).|Unconformably underlain by the Patchawarra and Epsilon Formations, and the Murteree and Roseneath Shales. Conformably overlain by the Arrabury Formation and the Callamurra Member.|Includes interbedded sandstone, siltstone, mudstone and shale, commonly in upwardly fining packages in the lower part.|12-MAY-16
18357|Toolachee Formation|69023|5|Briefly described|p81-82, p150-151|Permian|Permian|Cooper Basin. Oil and gas reserves.||Unit in Gidgealpa Group.||Disconformably overlies Daralingie Formation. Unconformably overlies Gidgealpa Group. Is overlain by Nappamerri Group.|Basal conglomerates with exotic clasts sourced from uplifted Warburton Basin.|
18357|Toolachee Formation|69454|5|Briefly described|p38:4|Changhsingian|Capitanian|Cooper Basin.||Gidgealpa Group.||||12-JUL-16
18357|Toolachee Formation|69594|5|Briefly described|p524|||Cooper Basin.||||Is overlain unconformably by Poolowanna Formation.||
18357|Toolachee Formation|69673|6|Mentioned|p153 fig 125|||||Gidgealpa Group||Overlain by Arrabury Formation, overlies Daralingie Formation||
18357|Toolachee Formation|69728|6|Mentioned|p285|||Cooper Basin.||Gidgealpa Group.||||
18357|Toolachee Formation|69797|5|Briefly described|p17 Fig.2|Late Permian|Late Permian|Age: Kazanian - Tatarian (approximated from figure). Geol. Prov: Cooper Basin.||Gidgealpa Group||||
18357|Toolachee Formation|69946|5|Briefly described|p9, p36, p54|Permian|Permian|Cooper Basin. Kazanian-Tatarian.||Uppermost unit in Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain conformably by Arrabury Formation (Nappamerri Group).||
18357|Toolachee Formation|69947|5|Briefly described|p13 Fig.7.2|Permian|Permian|Cooper Basin.||Gidgealpa Group.||||
18357|Toolachee Formation|69982|5|Briefly described|p14|||||||Unconformably overlies Mooracoochie Volcanics and Dullingari Group.|Includes basal conglomerate.|
18357|Toolachee Formation|70317|6|Mentioned|p33, 36|Late Permian|Late Permian|Cooper Basin. Vertical section showing fracture densities.||Gidgealpa Group.||Unconformably overlies Daralingie Formation (Gidgealpa Group). Is overlain by Callamurra Member (Arrabury Formation).||
18357|Toolachee Formation|70823|4|Described|iv, p1-p3, p6, p14|Changhsingian|Wuchiapingian|Cooper Basin. Hosts deep, dry coal seam gas. Seismic reflection, outcrop and palynological characteristics and coal thicknesses discussed. Up to 280m thick. Deposited in a meandering fluvial to deltaic environment. Hosts a commercial reservoir. Conformably overlain by the Callamurra Member of the Arrabury Formation. See also p25-p27, p39-p41, p53-p54, p58-p59, p61, p66, p70-p75, p78-p81, p83.||Gidgealpa Group||Disconformably overlies the Daralingie Formation. Unconformably overlies the Patchawarra Formation, Epsilon Formation and the Murteree Shale.|Interbedded fine to coarse-grained quartzose sandstone, mudstone, carbonaceous shale with thin coal seams and conglomerates.|
18357|Toolachee Formation|70824|4|Described|p1-p3, p5, p8-p9, p19, p28|Changhsingian|Wuchiapingian|Cooper Basin. Together with the Patchawarra Formation these are the richest, thickest and most extensive source rocks. Hosts deep dry coal seam gas. Up to 280m thick. Deposited in meandering fluvial to slightly deltaic environments. Outcrop and areal extent are discussed briefly in addition to source rock geochemistry. See also p30-p31, p66, p77, p84, p93-p95-p97, p99-p103, p108-p110, p113, p123.||||Unconformably overlies the Daralingie Formation. Overlain by the Callamurra Member (Arrabury Formation).|Interbedded fine to coarse-grained quartzose sandstone, mudstone, carbonaceous shale with thin coal seams and conglomerates.|
18357|Toolachee Formation|70946|5|Briefly described|p1087, p1089-1090|Permian|Permian|Cooper Basin. Hosts shallow and deep dry coal seam gas accumulations. Deposited in a meandering fluvial, partly deltaic environment.||Gidgealpa Group.||Unconformably overlies Daralingie Formation. Overlain by the Arrabury Formation.||08-OCT-18
18357|Toolachee Formation|71265|5|Briefly described|p589|Changhsingian|Wuchiapingian|Cooper Basin.||Gidgealpa Group.||Unconformably overlies Daralingie Formation. Is overlain unconformably by Arrabury Formation.||
18357|Toolachee Formation|71342|5|Briefly described|Ch5 p9, Ch5 p36, Ch5 p54|Tatarian|Kazanian|Cooper Basin. Palynological zone is given in fig 5.3 Ch5 p36. Deposited in a meandering fluvial or deltaic environment. See also Ch7 p13, Ch10 tbl 10.1, Ch10 p7, Ch10 p17-p20.||Gidgealpa Group||Unconformably overlies the Daralingie and Epsilon Formations. Conformably overlain by the Arrabury Formation.||
18357|Toolachee Formation|71701|5|Briefly described|p155|Changhsingian|Wuchiapingian|Cooper Basin.||Gidgealpa Group||Unconformably overlies the Daralingie Formation. Overlain by the Arrabury Formation.||09-FEB-23
18357|Toolachee Formation|72297|5|Briefly described|p697, p739, p742-743|Permian|Permian|Cooper Basin. Contains coal, but at too great a depth for economic extraction. One of the main petroleum source rocks within the Basin; also a reservoir. Also contains significant gas.||||||
18357|Toolachee Formation|73167|5|Briefly described|p662, p664, p666|late Permian|late Permian|Cooper Basin. Contains oil and gas, hydrocarbon source.||||Unconformably overlies the Daralingie Formation, underlies the Nappamerri Group.|Meandering fluvial to deltaic sediments.|
18357|Toolachee Formation|73244|6|Mentioned|p86|Permian|Permian|Cooper Basin. Meandering fluvial, deltaic environment. Oil, gas, and source rock.||||||
18357|Toolachee Formation|73251|6|Mentioned|p62|Lopingian|Guadalupian|Cooper Basin. Meandering fluvial depositional environment; deltaic in part. Hydrocarbon source rock that contains[?] gas and oil. Overlies the Daralingie Unconformity.||Gidgealpa Group||Overlain by Arrabury Formation including Callamurra Member.||
18357|Toolachee Formation|73343|5|Briefly described|p337-338|Late Permian|Late Permian|Cooper Basin. Source rock that hosts oil and gas. Reflect meandering fluvial to deltaic settings.||||Unconformably underlain by Daralingie Formation and Roseneath Shale. Overlain by Nappamerri Group including Callamurra Member.||
18357|Toolachee Formation|73479|5|Briefly described|p156 Fig.2, p159, p161, p163-166|Permian|Permian|Cooper Basin. Meandering fluvial to deltaic depositional environment. Most organic-rich source rock in basin. Associated with Daralingie Event.|ca 250 Ma|||Unconformably overlies Daralingie Formation, Roseneath Shale, underlies Nappamerri Group, Callamurra Member|Sands, shales and coals.|
18357|Toolachee Formation|73495|6|Mentioned|p499|Changhsingian|Wuchiapingian|||||||
18370|Toole Creek Volcanics|22460|4|Described|p446|||Also see Fig 1 p446 and p450.  Of the Soldiers Cap Group.||||||18-JAN-07
18370|Toole Creek Volcanics|22461|5|Briefly described|Fig 1 p464|||||||||
18370|Toole Creek Volcanics|22467|5|Briefly described|Fig 2 p431.|||Underlain by undifferentiated Toole Creek Volcanics/Mount Norna Quartzite.||||||18-JAN-07
18370|Toole Creek Volcanics|22483|6|Mentioned|p417|||||||||
18370|Toole Creek Volcanics|22513|6|Mentioned|p373|||Of the Soldiers Cap Group.||||||01-FEB-07
18370|Toole Creek Volcanics|22963|5|Briefly described|p69||Paleoproterozoic|Correlates with the upper sequence of the Georgetown (Qld) Etheridge Group and Bijerkerno Metasediments of the Willyama Supergroup.||||||22-JUL-13
18370|Toole Creek Volcanics|23071|5|Briefly described|p760|Statherian|Statherian|||||||
18370|Toole Creek Volcanics|23333|5|Briefly described|1114 Fig.1|Statherian|Statherian|Age: 1658+/-8Ma.||||||18-JAN-07
18370|Toole Creek Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1658+/-8Ma.||||||18-JAN-07
18370|Toole Creek Volcanics|23613|5|Briefly described|p725 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group.||||||07-NOV-08
18370|Toole Creek Volcanics|23901|5|Briefly described|p1685|Proterozoic|Proterozoic|Of the Soldiers Cap Group. Geological Province: Mount Isa Inlier.||||||
18370|Toole Creek Volcanics|23962|5|Briefly described|p1215 Fig. 2|||Geological Province: Mount Isa Inlier.  Of the Soldiers Cap Group.||||||16-DEC-04
18370|Toole Creek Volcanics|23971|5|Briefly described|p1407 Fig.1|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier. Of the Soldiers Cap Group||||||
18370|Toole Creek Volcanics|24032|6|Mentioned|p6 Tb. 1|||Metavolcanics.||||||
18370|Toole Creek Volcanics|24039|6|Mentioned|p463|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18370|Toole Creek Volcanics|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of Soldiers Cap Group. Overlies Mount Norna Quartzite. Age: 1658+/-8 Ma. Mafic. Geological Province: Eastern Fold Belt.||||||28-JAN-05
18370|Toole Creek Volcanics|24462|5|Briefly described|p297|Statherian|Statherian|Of the Soldiers Cap Group.  Age: 1658+/-8Ma (SHRIMP U-Pb).  Geological Province: Mount Isa Block.||||||
18370|Toole Creek Volcanics|33900|6|Mentioned|p17|||||||||
18370|Toole Creek Volcanics|35074|6|Mentioned|Fig.2|||||||||
18370|Toole Creek Volcanics|35295|2|Defined|p602|Precambrian|Precambrian|||||||
18370|Toole Creek Volcanics|35388|6|Mentioned|p89|||Also see Fig.10||||||
18370|Toole Creek Volcanics|37568|5|Briefly described|p81|||||||||
18370|Toole Creek Volcanics|38276|6|Mentioned|Fig.1|||||||||
18370|Toole Creek Volcanics|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18370|Toole Creek Volcanics|39425|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18370|Toole Creek Volcanics|39445|5|Briefly described|Table 2|||See also p35 and p42.||||||18-JAN-07
18370|Toole Creek Volcanics|39496|5|Briefly described|p7|||||||||
18370|Toole Creek Volcanics|39622|6|Mentioned|Fig.2|||||||||
18370|Toole Creek Volcanics|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
18370|Toole Creek Volcanics|40840|6|Mentioned|Map legend|||||||||
18370|Toole Creek Volcanics|41464|6|Mentioned|Map legend|Proterozoic||||||||
18370|Toole Creek Volcanics|41556|6|Mentioned|Map legend|Proterozoic||||||||
18370|Toole Creek Volcanics|41568|3|Fully described|p9|||||||||
18370|Toole Creek Volcanics|41791|5|Briefly described|p263|||||||||
18370|Toole Creek Volcanics|41978|3|Fully described|Table 1 p492|||||||||09-JUN-15
18370|Toole Creek Volcanics|43614|6|Mentioned|p19|||||||||
18370|Toole Creek Volcanics|43616|6|Mentioned|p7|||||||||
18370|Toole Creek Volcanics|44195|5|Briefly described|p345 Table 1,350|||U-Pb ages given.||||||
18370|Toole Creek Volcanics|45161|5|Briefly described|Table 12|||||||||
18370|Toole Creek Volcanics|45166|5|Briefly described|p25|||||||||
18370|Toole Creek Volcanics|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
18370|Toole Creek Volcanics|49041|6|Mentioned|Table 4|||||||||
18370|Toole Creek Volcanics|50100|5|Briefly described|p11, p20|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group.  Comprises amphibolite, metabasalt, metadolerite, BIF, chert, siltstone and quartzite.  See also misspelt Tool Creek Volcanics.||||||07-NOV-08
18370|Toole Creek Volcanics|50125|4|Described|p89|||Of the Soldiers Cap Group. Maximum Thickness: 2800m. Conformably overlies the Mount Norna Quartzite.||||||
18370|Toole Creek Volcanics|50332|5|Briefly described|p16, p21, p50, p61 Fig. 17|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group. Age: 1695-1600Ma. Geological Province: Cloncurry Subprovince. Comprise amphibolite, metabasalt, metadolerite, banded iron formation, chert, siltstone and quartzite.||||||07-FEB-11
18370|Toole Creek Volcanics|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Soldiers Cap Group. Mica schist, metasiltstone, quartzite, amphibolite.||||||
18370|Toole Creek Volcanics|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: ~1650Ma. Geological Province: eastern Mount Isa Block.||||||07-NOV-08
18370|Toole Creek Volcanics|61922|5|Briefly described|p9 Fig. 3, p10|||Uppermost unit of the Soldiers Cap Group. Overlies Mount Norna Quartzite. Geological Province: Mount Isa Inlier/Eastern Fold Belt. See also p12 Fig. 5.||||||
18370|Toole Creek Volcanics|61924|5|Briefly described|p44|||Mafic-dominated units. Geological Province: Eastern Fold Belt||||||
18370|Toole Creek Volcanics|61925|5|Briefly described|p56 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1658+/-8Ma. Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier. See also p57 Fig. 2.||||||07-NOV-08
18370|Toole Creek Volcanics|61926|5|Briefly described|p71 Fig. 1, p72 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1658+/-8Ma. Geological Province: Calvert Superbasin, Eastern Fold Belt, Mount Isa Inlier.||||||07-NOV-08
18370|Toole Creek Volcanics|61927|5|Briefly described|p95|||Metasedimentary unit consisting of feldspathic psammite and psammopelite intercalated with 50-200m thick sequences of carbonaceous muscovite schist and phyllite.||||||28-APR-06
18370|Toole Creek Volcanics|61929|5|Briefly described|p127, p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Soldiers Cap Group. Amphibolite, carbonaceous slate, scapolitic siltstone. Age: ~1625Ma; also 1670-1630Ma. . Geological Province: Calvert Superbasin. See also p129 Fig. 3.||||||07-NOV-08
18370|Toole Creek Volcanics|61936|5|Briefly described|p190 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the upper part of Soldiers Cap Group. Age: ca1658Ma. Geological Province: Eastern Fold Belt, Mount Isa Inlier. See also p195 Fig. 6.||||||07-NOV-08
18370|Toole Creek Volcanics|63866|5|Briefly described|p63-p64|||Records a range in metamorphic grade from amphibolite facies to granulite facies. Zircon populations are generally discordant, however the eight most concordant analyses provide an age of 1659 +/- 10 Ma and may be a stratigraphic age for this unit.||Soldiers Cap Group||||
18370|Toole Creek Volcanics|63884|5|Briefly described|p14|||Of Soldiers Cap Group. Faulted contact with Corella Formation. Greenschist grade.||||||
18370|Toole Creek Volcanics|64248|6|Mentioned|p38 Fig.5|Statherian|Statherian||1658 +/- 8 Ma.|Soldiers Cap Group.||||11-DEC-17
18370|Toole Creek Volcanics|64249|5|Briefly described|p84 Fig. 2, p104|Paleoproterozoic|Paleoproterozoic|Age: 1658Ma. Geological Province: Mount Isa Inlier.||||||22-APR-09
18370|Toole Creek Volcanics|64250|5|Briefly described|p10, p12, p24, p25 fig 10, p20, p22||||1658 +/-8 Ma|Soldiers Cap Group (top of).||Overlies Mount Norna Quartzite.|Basalt with some intercalated metasediments including siltstone, phyllite, schist and quartzite; minor banded calc-silicates, BIF, chert, jaspilite and slate.|13-MAY-14
18370|Toole Creek Volcanics|64252|5|Briefly described|p70 Fig. 1, p71|||Of Soldiers Cap Group. Geological Province: Mount Isa Inlier. Metavolcanic and metasedimentary rocks.||||||
18370|Toole Creek Volcanics|64725|6|Mentioned|p58 Fig.2. |||Mount Isa Inlier.||||||
18370|Toole Creek Volcanics|65387|5|Briefly described|p1, p3 Tb.1, p14-21, p82-85|Statherian|Statherian|Maximum deposition (detrital zircon) age.|1658 +/- 5 Ma SHRIMP zircon (Carson et al. 2008)|Unit in Soldiers Cap Group.||Suggested correlation with Answer Slate.|Basalt; includes grey feldspathic sandstone.|
18370|Toole Creek Volcanics|65396|4|Described|p7, p16-17, p28, p79, p82, p84, p101|Statherian|Statherian|See also p105, p124, p161, p175-178, p183, p188-190, p193, p195, p198, p241, p327, p333, p440. Isa Superbasin. Eastern succession, Cover Sequence 3. Cloncurry Fold Belt. Derived from strong fractionation of an Fe-picrite parental magma at 2 - 2.5 kb pressures. Detrital zircon sources listed.|1658 +/- 8 Ma (Page and Sun, 1998).|Soldiers Cap Group||Overlies Llewellyn Creek Formation,  Mount Norna Quartzite|Metadolerites, basalts with intercalated siltstone, phyllite, schist and quartzite. Minor banded calc-silicates, banded iron formation, jaspilite and slate.|04-APR-17
18370|Toole Creek Volcanics|65755|6|Mentioned|p2|||Part of Soldiers Cap Group in the north, Cloncurry Fault Zone.||||||
18370|Toole Creek Volcanics|65887|4|Described|p50-51|||Of Soldiers Cap Group. Conformably overlies Mount Norna Quartzite. ~2800m thick sequence of metadolerite and metabasalt, and minor interbedded quartzite, pelite and ironstone. Aged 1658 +/- 8 Ma (Page, 1998).||||||
18370|Toole Creek Volcanics|66913|5|Briefly described|p172, p176, p179, p181|||Considered to be part of Isa Superbasin.||||Overlies Soldiers Cap Group? Correlated with Marimo and Answer Slates.|Dominated by basalt lava flows; it also contains siltstone, mudstone, and quartzite. Multiply-deformed skarn-altered schist, phyllite black shale, metabasalt.|
18370|Toole Creek Volcanics|67323|4|Described|p18-19, p21, p26, p57, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Soldiers Cap/Kuridala/Etheridge Superbasin. Informally subdivided into basalt and amphibolite dominated and metasediment dominated units. High magnetic response. This age determination suggests a disconformity below this unit.|1658 +/- 5 Ma (MDA: Carson et al., 2008).|Soldiers Cap Group.||Correlated with Hampden Slate. Age-equivalent to Answer Slate. Intrudes Llewellyn Creek Formation and Mount Norna Quartzite.|Metabasalt and amphibolite with minor metasedimentary rocks; also common unmapped metadolerite sills and dykes. Fine-grained, dark grey metasiltstone, carbonaceous mudstone, chert, and subordinate metasandstone; minor metabasalt.|
18370|Toole Creek Volcanics|67498|6|Mentioned|p920 Fig.2|||||||||
18370|Toole Creek Volcanics|67539|4|Described|p13|Statherian|Statherian|Upper unit. Detrital zircon age.|c. 1690 - 1680 Ma|Of the Soldiers Cap Group.||Equivalent of the Starcross Formation. Underlain by the Mount Norna Quartzite?||
18370|Toole Creek Volcanics|68146|5|Briefly described|p201|||Age determination by Carson et al. (2008).|c.1650 Ma maximum depositional age.|Soldiers Cap Group.||Possible lateral equivalent to Starcross Formation.||
18370|Toole Creek Volcanics|68732|5|Briefly described|p163, p165 Fig.3, p169|Statherian|Statherian|Bouma Sequence. See also Toole Creek Formation in this paper. Detrital zircon maximum sedimentary depositional age.|1658 +/ 5 Ma.||||Comprises sandstone, siltstones, and shales.|01-DEC-17
18370|Toole Creek Volcanics|69056|4|Described|p2, p4-6, p13, p18, p21, p23, p28, p55|Statherian|Statherian|See also Reference images sheet, Time-Space plot sheet. Soldiers Cap Domain. Shown on the simplified surface and solid geology maps of the Quamby Project area. Modelling values listed. Maximum deposition age from sandstone.|1658 +/- 5 Ma (Carson et al., 2008).|Soldiers Cap Group.||Overlies Mount Norna Quartzite possibly disconformably. Probably intrudes Soldiers Cap Group. Equivalent to Hampden Slate.|Basalt flows; intervening fine-grained meta-sediments, including carbonaceous rocks and sandstone; mafic sills.|
18370|Toole Creek Volcanics|69370|5|Briefly described|p307, p309, p311, p314-315|Statherian|Statherian|Eastern Fold Belt, Mount Isa Block. Deformation described in detail.||Unit in Soldiers Cap Group.||Overlies Mount Norna Quartzite.|Dominantly volcanic unit composed of metadolerite and amphibolites.|25-JAN-19
18370|Toole Creek Volcanics|69582|6|Mentioned|p24|||Carpentaria Basin.|||||Metavolcanic rocks.|
18370|Toole Creek Volcanics|69591|4|Described|p38 Fig.2.22, p41, p43, p46, p55|||Soldiers Cap Domain, Calvert Superbasin. Part of the Gun Supersequence. Deep marine sediments. Age is maximum depositional age of the lower part sandstones.|1658 +/- 5 Ma (Carson et al., 2008).|Soldiers Cap Group.||Overlies Mount Norna Quartzite. Intrudes Llewellyn Creek Formation and Mount Norna Quartzite (Soldiers Cap Group). Coeval with Answer Slate.|The lower part includes sandstones. The upper part consists of basalt flows interbedded with largely metapelitic, commonly carbonaceous rocks intruded by mafic sills. p55 lists amphibolite, metamorphosed chert and siltstone, phyllite, slate.|
18370|Toole Creek Volcanics|69952|5|Briefly described|p4-5, p51, p53|||Maximum depositional age for sandstone in the lower part of this unit. A recrystallised felsic rock in this unit has an age of 1654 +/- 4 Ma. The suggested direct correlation with the Kuridala Group, made by eg Hutton and Withnall (2013), appears to be refuted by this latest age determination of the Hampden Slate of 1684.5 +/- 5.0 Ma (Cross et al., 2015).|<1658 +/- 5 Ma (Carson et al., 2008).|||||
18370|Toole Creek Volcanics|70353|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The two facies, broadly volcanic and sedimentary, are mapped separately.||Soldiers Cap Group.||Overlies Mount Norna Quartzite.|Metabasalt and amphibolite with minor metasedimentary rocks; also commonly unmapped metadolerite sills and dykes. Fine-grained, dark grey metasiltstone, carbonaceous mudstone, chert and subordinate metasandstone; minor metabasalt.|
18370|Toole Creek Volcanics|70354|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The two facies, broadly volcanic and sedimentary, are mapped separately.||Soldiers Cap Group.||Overlies Mount Norna Quartzite.|Metabasalt and amphibolite with minor metasedimentary rocks; also commonly unmapped metadolerite sills and dykes. Fine-grained, dark grey metasiltstone, carbonaceous mudstone, chert and subordinate metasandstone; minor metabasalt.|
18370|Toole Creek Volcanics|70570|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Soldiers Cap Group.||Overlies Mount Norna Quartzite.|Metabasalt, amphibolite, fine-grained, dark grey metasiltstone, carbonaceous mudstone, chert, and subordinate metasandstone. Common unmapped metadolerite sills and dykes.|05-MAY-16
18370|Toole Creek Volcanics|70571|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain. Includes two unnamed members: fine grained, metasiltstone and carbonaceous mudstone chert and metasandstone; metabasalt and amphibolite with minor metasedimentary rocks.||Soldiers Cap Group.|Includes two unnamed members.||Metabasalt, amphibolite, fine grained metasiltstone, carbonaceous mudstone, chert and subordinate metasandstone.|
18370|Toole Creek Volcanics|70572|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group.|||Metabasalt, amphibolite, fine grained metasiltstone, carbonaceous mudstone, chert and subordinate metasandstone.|20-JAN-22
18370|Toole Creek Volcanics|70573|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Soldiers Cap Domain.||Soldiers Cap Group|||Metabasalt, amphibolite, fine grained metasiltstone, carbonaceous mudstone, chert and subordinate metasandstone.|
18370|Toole Creek Volcanics|70858|6|Mentioned|p29, 31|Paleoproterozoic|Paleoproterozoic|Tommy Creek Block, Isan Superbasin. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.|1658 +/- 8 Ma.|||||
18370|Toole Creek Volcanics|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1658+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
18370|Toole Creek Volcanics|71799|5|Briefly described|p150 fig 2, p151 fig 3|Statherian|Statherian|Eastern Fold Belt/ Kalkadoon-Leichardt Block. Age constrained in: Baker et al, 2010; Carson et al, 2009; Carson et al, 2011; Neumann and Kositcin 2011; and Page and Sun, 1998. Geochemistry is discussed. See also p153 tbl 1, p155, p157 fig 5, p158, p161.|1658 +/- 5 Ma (SHRIMP U-Pb)|||Overlies the Soldiers Cap Group.|Basalt, dolerite, gabbro or amphibolite.|
18370|Toole Creek Volcanics|72461|6|Mentioned|p6|||Mount Isa Eastern Fold Belt.||||||
18370|Toole Creek Volcanics|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Snake Creek-Soldiers Cape Domain.|1658+/-8 Ma maximum depositional age||||Carbonaceous siliciclastics, minor mafic extrusives.|
18375|Toolebuc Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 3-75m thick. Characteristic high gamma response. Contains abundant bivalves, fish skeletons and teeth, radiolarians, globigerinids and dinoflagellates.|||||Carbonaceous and calcareous mudstone and limestone with minor thin interbeds of fine-grained calcareous labile sandstone and siltstone; local 10m thick oil-shale horizon in N.|
18375|Toolebuc Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Shale and siltstone with minor shoreface sandstone.|
18375|Toolebuc Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Albian|Albian|In Eromanga Basin.||||||
18375|Toolebuc Formation|22464|5|Briefly described|p9||Early Cretaceous|In the Eromanga Basin. Overlies Wallumbilla Formation.||||||12-DEC-06
18375|Toolebuc Formation|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Albian|Albian|Oil shales occur. Together with Allaru Mudstone thickness is ~100m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|22865|4|Described|p295,Table22.1p296-7|Cenomanian|Albian|||||||
18375|Toolebuc Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlain by Allaru Mudstone, underlain by Wallumbilla Formation.||||||01-FEB-07
18375|Toolebuc Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23031|5|Briefly described|31|||||||||
18375|Toolebuc Formation|23056|6|Mentioned|12 table 2|||||||||
18375|Toolebuc Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group) - not clear in legend however.||||||14-DEC-06
18375|Toolebuc Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The formation is restricted to the northern and western STRZELECKI.||||||
18375|Toolebuc Formation|23356|5|Briefly described|26 Tab.2|Albian|Albian|||||||
18375|Toolebuc Formation|23375|4|Described|Fig2 p265, 266||Albian|Laterally equivalent to lower Oodnadatta Formation. In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|23425|4|Described|Table 9.7 p394||Albian|see also p378. Of Rolling Downs Group. Overlain by Allaru Mudstone; underlain by Wallumbilla Formation. Carpentaria Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23430|4|Described|p522 + p524 Table 14.7|||In the Eromanga Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23431|5|Briefly described|p543|||||||||
18375|Toolebuc Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
18375|Toolebuc Formation|23864|6|Mentioned|p128|Albian|Albian|||||||
18375|Toolebuc Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
18375|Toolebuc Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
18375|Toolebuc Formation|23982|5|Briefly described|p12|Cretaceous|Cretaceous|Of the Rolling Downs Group. Geological Province: Eromanga Basin. See also page 35 Fig.7.||||||
18375|Toolebuc Formation|23986|5|Briefly described|p71|||||||||
18375|Toolebuc Formation|24048|5|Briefly described|p76|||||||||
18375|Toolebuc Formation|24085|5|Briefly described|p33, p36, p38|Albian|Albian|Geological Province: Eromanga Basin.||||||16-SEP-08
18375|Toolebuc Formation|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24201|5|Briefly described|p379|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
18375|Toolebuc Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24226|5|Briefly described|p391|Albian|Albian|Age: Late Albian.||||||
18375|Toolebuc Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Allaru Formation. Underlying Unit: Wallumbilla Formation. Maximum Thickness: <35m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|29394|6|Mentioned|p145|||Cretaceous.||||||
18375|Toolebuc Formation|30584|4|Described|Table 1|||||||||
18375|Toolebuc Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|31121|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|31165|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|31168|6|Mentioned|p10|||||||||
18375|Toolebuc Formation|32314|6|Mentioned|Fig. 4|||||||||
18375|Toolebuc Formation|32705|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|33017|6|Mentioned|p1|||See also p8.||||||12-DEC-06
18375|Toolebuc Formation|33075|4|Described|p451|||Type section p455.||||||12-DEC-06
18375|Toolebuc Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
18375|Toolebuc Formation|33176|6|Mentioned|p175|||||||||
18375|Toolebuc Formation|33177|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|33178|6|Mentioned|p11|||||||||
18375|Toolebuc Formation|33179|4|Described|p11|||||||||
18375|Toolebuc Formation|33368|6|Mentioned|p27|||Refers Smart (1972).||||||
18375|Toolebuc Formation|33414|6|Mentioned|p212,213,Tb.|||Part of Wilgunya Sub-group.||||||
18375|Toolebuc Formation|33772|6|Mentioned|p13|||||||||
18375|Toolebuc Formation|33773|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|33900|6|Mentioned|p21|||||||||
18375|Toolebuc Formation|34811|4|Described|Table 1|||||||||
18375|Toolebuc Formation|35220|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|35239|6|Mentioned|p258|||||||||
18375|Toolebuc Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35457|6|Mentioned|p623|||||||||
18375|Toolebuc Formation|35560|4|Described|p291|||||||||
18375|Toolebuc Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
18375|Toolebuc Formation|35793|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|35811|5|Briefly described|Table 3|||Uranium exploration discussed p556.||||||12-DEC-06
18375|Toolebuc Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
18375|Toolebuc Formation|35936|6|Mentioned|p615|||||||||
18375|Toolebuc Formation|36012|3|Fully described|Table 5|||See also p18.||||||12-DEC-06
18375|Toolebuc Formation|36110|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|36243|6|Mentioned|Table 6A|||||||||
18375|Toolebuc Formation|36251|4|Described|p3|||||||||
18375|Toolebuc Formation|36331|6|Mentioned|p92|||||||||
18375|Toolebuc Formation|36552|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36571|6|Mentioned|p95|||||||||
18375|Toolebuc Formation|36690|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36713|5|Briefly described|p361|||||||||
18375|Toolebuc Formation|36910|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36912|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|36922|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|37287|6|Mentioned|p36|||||||||
18375|Toolebuc Formation|37608|3|Fully described|Table 1|||||||||
18375|Toolebuc Formation|37776|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|38011|6|Mentioned|p126|||||||||
18375|Toolebuc Formation|38199|5|Briefly described|p426|||Palynology||||||
18375|Toolebuc Formation|38218|4|Described|p285|||||||||
18375|Toolebuc Formation|38226|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|38325|4|Described|p265|||||||||
18375|Toolebuc Formation|38372|6|Mentioned|p647|||||||||
18375|Toolebuc Formation|38373|6|Mentioned|p618|||||||||
18375|Toolebuc Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
18375|Toolebuc Formation|38779|6|Mentioned|p7|||||||||
18375|Toolebuc Formation|38780|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|38814|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlain by Allaru Mudstone.||||||25-AUG-04
18375|Toolebuc Formation|39070|4|Described|p365|||||||||
18375|Toolebuc Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,12-16 etc. Correlation.||||||12-DEC-06
18375|Toolebuc Formation|39445|5|Briefly described|Table 11|||||||||
18375|Toolebuc Formation|39478|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39480|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|39481|6|Mentioned|p180|||||||||
18375|Toolebuc Formation|39482|6|Mentioned|Fig.7|||||||||
18375|Toolebuc Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39575|6|Mentioned|p103|||||||||
18375|Toolebuc Formation|39708|4|Described|p477|||||||||
18375|Toolebuc Formation|39754|6|Mentioned|p1690|||||||||
18375|Toolebuc Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39846|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|39847|5|Briefly described|p39|||||||||
18375|Toolebuc Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39914|6|Mentioned|p3|||||||||
18375|Toolebuc Formation|39942|6|Mentioned|p463|||||||||
18375|Toolebuc Formation|39943|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|39989|6|Mentioned|p426|||||||||
18375|Toolebuc Formation|40121|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|40167|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|40199|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|40249|6|Mentioned|p41|||||||||
18375|Toolebuc Formation|40322|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|40452|6|Mentioned|p2|||||||||
18375|Toolebuc Formation|40648|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|40670|6|Mentioned|Fig.9|||||||||
18375|Toolebuc Formation|40675|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|40687|6|Mentioned|Table 3|||||||||
18375|Toolebuc Formation|40719|5|Briefly described|p61|||||||||
18375|Toolebuc Formation|40771|5|Briefly described|p429|||||||||
18375|Toolebuc Formation|40801|6|Mentioned|p46|||||||||
18375|Toolebuc Formation|40926|6|Mentioned|p18|||||||||
18375|Toolebuc Formation|41012|3|Fully described|p137|||||||||
18375|Toolebuc Formation|41036|6|Mentioned|p220|||||||||
18375|Toolebuc Formation|41052|6|Mentioned|p87|||||||||
18375|Toolebuc Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41061|6|Mentioned|p19|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41062|6|Mentioned|Fig.5|||||||||
18375|Toolebuc Formation|41063|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|41064|6|Mentioned|p62|||||||||
18375|Toolebuc Formation|41084|5|Briefly described|Fig.2|||||||||
18375|Toolebuc Formation|41086|3|Fully described|p101|||See also Fig.3||||||
18375|Toolebuc Formation|41087|3|Fully described|p121|||||||||
18375|Toolebuc Formation|41088|4|Described|p141|||||||||
18375|Toolebuc Formation|41089|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|41097|6|Mentioned|p166|||||||||
18375|Toolebuc Formation|41117|4|Described|p434|||||||||
18375|Toolebuc Formation|41121|6|Mentioned|p179|||||||||
18375|Toolebuc Formation|41125|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|41165|5|Briefly described|p362, p368|||Mention Fig.20||||||
18375|Toolebuc Formation|41174|4|Described|p117|||||||||
18375|Toolebuc Formation|41175|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41176|6|Mentioned|p206|||See also Table 2||||||
18375|Toolebuc Formation|41177|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41178|6|Mentioned|p241|||||||||
18375|Toolebuc Formation|41179|6|Mentioned|p255|||||||||
18375|Toolebuc Formation|41180|5|Briefly described|p267|||||||||
18375|Toolebuc Formation|41181|6|Mentioned|p273|||||||||
18375|Toolebuc Formation|41182|5|Briefly described|p300|||||||||
18375|Toolebuc Formation|41183|6|Mentioned|p310|||||||||
18375|Toolebuc Formation|41184|6|Mentioned|p328|||||||||
18375|Toolebuc Formation|41187|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41196|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41198|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|41214|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41216|6|Mentioned|Fig.18|||||||||
18375|Toolebuc Formation|41219|6|Mentioned|p338|||||||||
18375|Toolebuc Formation|41266|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41306|6|Mentioned|p4|||||||||
18375|Toolebuc Formation|41307|6|Mentioned|p5|||||||||
18375|Toolebuc Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41482|6|Mentioned|p37|||||||||
18375|Toolebuc Formation|41483|6|Mentioned|p49|||||||||
18375|Toolebuc Formation|41523|3|Fully described|p279|||||||||
18375|Toolebuc Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41568|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|41707|6|Mentioned|p164|||||||||
18375|Toolebuc Formation|41724|6|Mentioned|p383|||||||||
18375|Toolebuc Formation|42061|4|Described|p155|||||||||
18375|Toolebuc Formation|42067|4|Described|Appendix 2|||||||||
18375|Toolebuc Formation|42071|6|Mentioned|p117|||||||||
18375|Toolebuc Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18375|Toolebuc Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18375|Toolebuc Formation|42374|6|Mentioned|p435|Albian||||||||
18375|Toolebuc Formation|42397|6|Mentioned|Fig.2 P3|||||||||
18375|Toolebuc Formation|42402|5|Briefly described|p115, 116|||||||||
18375|Toolebuc Formation|42429|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|42446|4|Described|p13|||||||||
18375|Toolebuc Formation|42447|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
18375|Toolebuc Formation|42520|5|Briefly described|p6|||||||||
18375|Toolebuc Formation|42538|5|Briefly described|Fig. 25.2 P325|||||||||
18375|Toolebuc Formation|42585|5|Briefly described|p79|||||||||
18375|Toolebuc Formation|42588|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42637|4|Described|p11|||||||||
18375|Toolebuc Formation|42673|5|Briefly described|Fig.2, P184|||||||||
18375|Toolebuc Formation|42746|6|Mentioned|Fig.6 P8|||||||||
18375|Toolebuc Formation|42749|6|Mentioned|Fig.2 P27|||||||||
18375|Toolebuc Formation|42804|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
18375|Toolebuc Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18375|Toolebuc Formation|43004|5|Briefly described|Table 1,p179|||||||||
18375|Toolebuc Formation|43105|6|Mentioned|p15|||||||||
18375|Toolebuc Formation|43114|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|43122|5|Briefly described|p29|||see also Fig. 2.||||||
18375|Toolebuc Formation|43591|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|43602|6|Mentioned|191|||In Eromanga Basin. Of the Rolling Downs Group.||||||12-DEC-06
18375|Toolebuc Formation|43630|6|Mentioned|p70|||also Fig.4||||||
18375|Toolebuc Formation|44112|6|Mentioned|p82|||||||||
18375|Toolebuc Formation|44133|5|Briefly described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|44291|14|Not recorded|p14|||||||||
18375|Toolebuc Formation|45145|3|Fully described|Table 5|||||||||
18375|Toolebuc Formation|45161|6|Mentioned|p67|||||||||
18375|Toolebuc Formation|46791|4|Described|p47|||||||||
18375|Toolebuc Formation|46872|6|Mentioned|p105|||||||||
18375|Toolebuc Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
18375|Toolebuc Formation|47042|4|Described|p171|||||||||
18375|Toolebuc Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|48770|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|49010|6|Mentioned|Fig.4|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49254|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49273|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49278|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49330|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49338|14|Not recorded|?|||||||||
18375|Toolebuc Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Contains calcareous bituminous shale (oil shale).  Geological Province: Carpentaria and Eromanga Basins.||||||
18375|Toolebuc Formation|50332|5|Briefly described|p22, p93, p96|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone. Also contains calcareous bituminous shale (oil shale).||||||07-FEB-11
18375|Toolebuc Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Limestone, calcareous sandstone.||||||
18375|Toolebuc Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Lateral to Oodnadatta Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
18375|Toolebuc Formation|61312|5|Briefly described|p66, p73|Albian|Aptian|Of the Rolling Downs Group. In Queensland it consists of carbonaceous and bitumous shale and siltstone with limestone lenses. In Queensland, overlies Wallumbilla Formation and is overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||16-JUN-06
18375|Toolebuc Formation|61544|5|Briefly described|p374.|Albian|Albian|Eromanga Basin. Contains marine oil shales which are geochemically similar to asphaltite strandings along the Bight coast.|||||Includes marine oil shales.|
18375|Toolebuc Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
18375|Toolebuc Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
18375|Toolebuc Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
18375|Toolebuc Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
18375|Toolebuc Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~101-~98Ma. Geological Province: Southern Cape York and Burketown Depression.||||||01-MAR-10
18375|Toolebuc Formation|63979|2|Defined|p50, Fig. 44|Albian|Albian|Previously Toolebuc Member (Wilgunya Fm). Conformable over Wallumbilla Fm; overlain by Allaru Mudstone. Max.thick: 65m. Predominantly mudstone with thin layers of siltstone, sandstone and conglomerate, towards top; also contains limestone (incl. coquinite)||||||09-APR-13
18375|Toolebuc Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - oil shale. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Underlies Allaru Mudstone; overlies Wallumbilla Formation.||11-DEC-15
18375|Toolebuc Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
18375|Toolebuc Formation|64820|5|Briefly described|pS6 Fig. 4|Late Albian|Late Albian|Of the Rolling Downs Group. Carbonaceous to calcareous silt-claystone with minor sandstones. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
18375|Toolebuc Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
18375|Toolebuc Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 52 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Shale.|Limestone, calcareous bituminous shale.|
18375|Toolebuc Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Wallumbilla Formation. Overlain by Allaru Mudstone.||||||08-MAR-12
18375|Toolebuc Formation|65489|5|Briefly described|p49, p55, p58, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 60m thick. Oil shale potential.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66529|5|Briefly described|p10, p12, p16-17, p41, p92    |Mesozoic|Mesozoic|Eromanga Basin. Previously investigated for oil shale. An ideal in situ reductant for U systems.|c.107 Ma.|Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Significant organic content. Black shale.|
18375|Toolebuc Formation|66623|6|Mentioned|p264.|||||||Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66915|5|Briefly described|p6 Fig.3, p16|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins. In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||||Includes a thin competent unit of calcareous and bituminous shale, and limestone (a distinct and laterally persistent seismic reflection for correlation).|
18375|Toolebuc Formation|67323|5|Briefly described|p39, p81, p85-89, p93-94, p95 Fig.12.5|Early Cretaceous|Early Cretaceous|See also p96, GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Widespread shallow-marine deposits. Hydrocarbon exploration target in the Eromanga Basin; bituminous shale occurs throughout its extent. Considered prospective for U in the Carpentaria Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale, limestone.|
18375|Toolebuc Formation|67402|4|Described|p108, p109, p112|Albian|Albian|Eromanga Basin. Generally only between 20-45m thick but may be up to 65m thick. Deposited in a restricted marine environment. See also  p113 fig ERO12, p123, p176, p177, p179 fig CRP/KRM6, p180, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Mudstone dominated succession that also contains limestone that is subordinate to calcareous, bituminous siltstone, labile sandstone and shale.|
18375|Toolebuc Formation|67561|6|Mentioned|p53 Fig.3|||||||||
18375|Toolebuc Formation|67784|5|Briefly described|p25-26, p28-29, p31-32, p34|Albian|Albian|6-25m thick. Carpentaria, northern Eromanga Basins. Appears as Toolebuc Limestone in Tb.1 (p28). Euxinic facies.||Wilgunya Subgroup.||Overlain by Allaru Mudstone. Overlies Ranmoor Member/Coreena Member (Wallumbilla Formation). Is correlated with Oodnadatta Formation|Contains distinctive Inoceramus coquinites and oil shale.|08-FEB-18
18375|Toolebuc Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
18375|Toolebuc Formation|68206|5|Briefly described|p31, 33|Albian|Albian|NE Eromanga Basin. See also reference to Toolebuc Limestone (p32).||||Overlies Ranmoor Member (Wallumbilla Formation). Is overlain by Allaru Formation.|Limestone; distinctive Inoceramus coquinites and oil shale.|
18375|Toolebuc Formation|68279|6|Mentioned|p19|||Galilee Basin stratigraphic cross-section, and mineralogy table.||||||
18375|Toolebuc Formation|68307|5|Briefly described|p92|Early Cretaceous|Early Cretaceous|Eromanga-Carpentaria Basin. Organic-rich. Forms a strong reflective seismic horizon.||||||
18375|Toolebuc Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.||
18375|Toolebuc Formation|68731|6|Mentioned|pp209-211|||||||||
18375|Toolebuc Formation|68734|5|Briefly described|p218 Fig.2|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
18375|Toolebuc Formation|68821|5|Briefly described|p292 Fig.1, p295, p296, p298|Cenomanian|Cenomanian|Lower Cretaceous age. Parallic to marine sediments. Contains ubiquitous disseminated pyrite. Equivalent in age to the Surat Siltstone.|101 - 98 Ma|Of the Rolling Downs Group.|||Dominantly organic-rich black shale with thin (< 3 cm) beds of limestone.|
18375|Toolebuc Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Albian|||||||
18375|Toolebuc Formation|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
18375|Toolebuc Formation|69206|6|Mentioned|p2|Cretaceous|Cretaceous||||||Immature oil shale.|
18375|Toolebuc Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Albian|Upper Albian|Carpentaria Basin. The carbonaceous mudstones are the best potential source rocks in the basin.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Carbonaceous mudstone, siltstone and claystone.|
18375|Toolebuc Formation|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
18375|Toolebuc Formation|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
18375|Toolebuc Formation|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,15-18|Albian|Albian|Casey (1959). Eromanga, Carpentaria Basins. Widespread occurrence in drillholes. Shallow-marine deposits. Up to 65m thick. This unit and the Allaru Mudstone are together equivalent to the middle and upper part of Oodnadatta Formation. Has a distinctive, strong gamma signature in wireline logs. Regarded as an oil shale in the NE part of the Basin in Qld. A rich oil-gas source rock, the mudstone typically has a high TOC, generally 9-20%, locally 35%, derived from planktonic algae and cyanobacterial mats; it is an attractive oil shale and unconventional petroleum exploration target. Contains diverse fossil assemblages.||Wilgunya Subgroup.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Dark grey to black mudstone which may be carbonaceous, calcareous or pyritic, with thin layers of siltstone; subordinate labile sandstone, limestone, marl and conglomerate.|12-JUL-16
18375|Toolebuc Formation|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone.|
18375|Toolebuc Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Wallumbilla Formation. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|69594|4|Described|p518-519, p521-522, p526, p529-530, p533|Albian|Albian|See also p574. Carpentaria, Eromanga Basins. A thin, isochronous unit up to 65m thick; generally 20-45m. Represents maximum marine conditions within an epeiric basin system. Early late Albian. Contains oil shales; may also be prospective for shale gas. Has a distinct and strong gamma signature. Contains spectacular vertebrate fossils (listed).||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Coquinitic limestone, nodular limestone, oil shale, kerigenous shale, with minor siltstone and labile sandstone.|
18375|Toolebuc Formation|69673|6|Mentioned|p12 t5, p159, p160, p164, p165|||Prospective for unconventional hydrocarbons. Potential oil/gas source rock.||Wilgunya Subgroup||Overlain by Allaru Mudstone, overlies Wallumbilla Formation|Mudstone with thin layers of siltstone and subordinate labile sandstone, limestone, marl and conglomerate.|
18375|Toolebuc Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Toolebuc Fm.||||||
18375|Toolebuc Formation|69946|3|Fully described|p23-26, p57, p94|Albian|Albian|Originally Toolebuc Member (Casey, 1959) of the Wilgunya Formation. Later upgraded to Toolebuc Limestone (Vine et al., 1967), then defined as Toolebuc Formation by Senior et al. (1975). Casey's type section, outcrop on the Boulia-Winton Road 7 miles (11.3km) E of the Hamilton Hotel, was replaced because of poor outcrop by Senior et al. (1975) by the interval 25.3 - 35.8 m in BMR Boulia 3A. A reference section was also assigned to Boulia 3 (25 - 36m). High gamma ray response: its role in identifying Wallumbilla Formation mis-correlations from Qld into SA is discussed. Up to 50m thick. Wireline log correlations.||||Conformably overlies Wallumbilla Formation. Passes laterally into Oodnadatta Formation. Is overlain conformably by Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains; dark grey fossiliferous mudstone with coquinite comprising large bivalve shells; dark grey mudstone. Bituminous shales in the type section; local oil shale origins.|
18375|Toolebuc Formation|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
18375|Toolebuc Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale and limestone.|
18375|Toolebuc Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|20-JAN-22
18375|Toolebuc Formation|70574|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|18-JAN-22
18375|Toolebuc Formation|70821|5|Briefly described|p21, p33, p80|Early Cretaceous|Early Cretaceous|Eromanga Basin. Absent in the southern Thomson region.||Rolling Downs Group.||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70823|5|Briefly described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a restricted, stratified and anoxic marine environment. Hosts an oil shale source rock.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Formation.||
18375|Toolebuc Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil shale source rocks.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||
18375|Toolebuc Formation|70836|6|Mentioned|p474|Albian|Albian|||||Coeval with Griman Creek Formation.||
18375|Toolebuc Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
18375|Toolebuc Formation|71059|6|Mentioned|p6 Fig.5|||Eromanga Basin.||||||
18375|Toolebuc Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||24-OCT-19
18375|Toolebuc Formation|71342|3|Fully described|Ch4 p25, Ch5 p23-p25|Late Albian|Middle Albian|Eromanga Basin. Originally named by Casey (1959) the Toolebuc Member of the Wilgunya Formation. Vine et al (1967) subsequently upgraded the member to formation status as the Toolebuc Limestone. Senior et al (1975) redefined the Limestone as the Toolebuc Formation. The type section for this unit was originally assigned to outcrop on the Boulia-Winton Road by Casey (1959). The BMR defined a new type section in Boulia 3A due to poor outcropping of the original section. A reference section was also given. Distribution and wireline log characteristics are given. A maximum thickness of 50m is recorded in Haddon Downs 1 in the northern Cooper region. Age derived from fossil assemblage and palynological studies. Interpreted to have been deposited in a restricted marine environment. Spore-pollen zone is given in Ch5 p57. See also Ch5 p57, Ch6 p9, Ch7 p13, Ch12 p12, Ch12 p14.||||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains, dark grey fossiliferous mudstone with coquinite containing abundant bivalves and bituminous shales.|
18375|Toolebuc Formation|71382|5|Briefly described|p4, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 156.65m-199.87m for a total of 43.22m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p21. See also p21, p23, p25, p27, App 3, 4.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone and calcareous mudstone.|
18375|Toolebuc Formation|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
18375|Toolebuc Formation|71855|4|Described|p1-p2, p4-p6, p9-p11, p13, p15, p18, p20|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria basins. This unit has three distinct lithofacies which are described. In places the contact with the underlying Wallumbilla Formation is faulted or disconformable. This unit is highly organic rich and has good source rock charactersitcs. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure, geochemistry and source rock potential are discussed. Typically greater than 15m thick. See also p22-p35, p42-p44, p47-p50, p52-p53, p56-p57, p61-p64, p66-p68, p73-p75.||Rolling Downs Group||Conformably (gradationally) overlies the Wallumbilla Formation. Conformably (gradationally) overlain by the Allaru Mudstone. Overlain by the Mackunda Formation.|Calcareous mudstone, coquinitic mudstone and organic-rich, slightly calcareous mudstone without calcite laminae.|
18375|Toolebuc Formation|71863|4|Described|p1-p18|Albian|Albian|Eromanga and Carpentaria basins. Originally defined as the Toolebuc Limestone by Vine et al. (1967). Subsequently this unit was redefined by Senior et al (1975) as the Toolebuc Formation due to recognition of significant mudstone component. The type section is defined in BMR Boulia 3A (Burger, 1974; Senior et al., 1975). Deposited during a marine incursion. Mudstone may contain laminae of carbonate form from bivalve remains Inoceramus and Aucellina (Ozimic, 1986). Deposited in a restricted, oxygen depleted marine environment. Wireline log characteristics, geochemistry, sedimentary facies, fossil assemblage, petroleum resources and mineralisation are discussed. Equivalent to the Wooldrige Limestone Member and Urisino beds.||Rolling Downs Group||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone. Equivalent to the Wooldridge Limestone Member and Urisino beds.|Laminated calcareous and kerogenous mudstone, minor coquinite and limestone, labile sandstone and oil shale.|01-MAY-19
18375|Toolebuc Formation|72297|5|Briefly described|p712, p721, p728, p746, p751-753, p755|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria Basins. Julia Creek area; occurs north as far as 16 degrees S. Oxidised oil shales in the upper part produce soft oxide coquina, with associated large molybdenum and vanadium resources. Hosts a large gypsum deposit at Hughenden; other localities mentioned. An excellent though immature hydrocarbon source rock. Very high potential shale oil resources (perhaps the most extensive in Australia) despite very low grade; eg Julia Creek oil shale deposit (described).||||Conformably overlies the Ranmoor Member (Wallumbilla Formation). Is overlain conformably by the Allaru Mudstone.|A flat-lying unit comprising an upper, coarse limestone-clay-oil shale unit and a lower, fine carbonate-clay-oil shale unit. Contains mudstones rich in organic kerogenous material.|
18375|Toolebuc Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Coreena and Ranmoor Members (Wallumbilla FZ). Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|72799|6|Mentioned|p27|||||||||
18375|Toolebuc Formation|72913|6|Mentioned|p8.|||Three wells intersected this cover unit.||||||
18375|Toolebuc Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
18375|Toolebuc Formation|73083|6|Mentioned|p58, p62-63|||||||Underlain by the Wallumbilla Formation.|Includes shale and subordinate limestone.|
18375|Toolebuc Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquitard with potential shale gas/oil play.||Rolling Downs Group||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|73249|5|Briefly described|p319, p321, p323|Albian|Albian|Eromanga Basin. Deposited in a marine environment.||||Overlies the Wallumbilla Formation, underlies the Allaru Mudstone, lateral equivalent of the Coorikiana Sandstone.|Mudstone.|
18375|Toolebuc Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18375|Toolebuc Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 103 Ma|||Overlies Wallumbilla Formation, underlies Allaru Mudstone||
18375|Toolebuc Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
18404|Toondahra Granite|23799|4|Described|p98, p11 Tb. 1|Triassic|Triassic|Very fine-grained biotite leucogranite. Of the South-east Queensland Volcanic and Plutonic Intrusives.||||||18-AUG-08
18404|Toondahra Granite|23800|5|Briefly described|Map Legend|Late Triassic|Late Triassic|||||||
18404|Toondahra Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
18404|Toondahra Granite|33774|3|Fully described|p73|||Intrudes Aranbanga Beds.||||||18-AUG-08
18404|Toondahra Granite|33905|2|Defined|p266|Middle Triassic|Middle Triassic|||||||
18404|Toondahra Granite|34998|6|Mentioned|p347|||||||||
18404|Toondahra Granite|36333|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
18404|Toondahra Granite|36926|6|Mentioned|p176|||||||||
18404|Toondahra Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
18404|Toondahra Granite|39445|5|Briefly described|Table 12|||||||||
18404|Toondahra Granite|39632|6|Mentioned|p224|||||||||
18404|Toondahra Granite|39845|6|Mentioned|p20|||||||||
18404|Toondahra Granite|43008|5|Briefly described|map legend|||||||||
18404|Toondahra Granite|60371|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Very fine-grained biotite leucogranite.||||||18-AUG-08
18404|Toondahra Granite|64398|5|Briefly described|Map legend|Late Triassic|Late Triassic|Pink to cream, fine- to medium-grained peralkaline arfvedsonite syenogranite.||||||14-AUG-08
18404|Toondahra Granite|65003|5|Briefly described|p1, p5, p26|Triassic|Triassic|||||Intrudes the Maronghi Creek beds.||
18404|Toondahra Granite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
18404|Toondahra Granite|68679|5|Briefly described|p415, p428-429|Late Triassic|Late Triassic|Northern New England Orogen. This c.215 Ma age is recalculated from Withnall (1971).|215 +/- 6 Ma (K-Ar arfvedsonite age).|||Intrudes the Aranbanga Volcanic Group. Is intruded by Farquharson Granite.|Fine- to medium-grained, peralkaline arfvedsonite syenogranite or fine- to medium-grained, equigranular, leucocratic biotite granite with strong NE and NW jointing and abundant rhyolite dykes.|
18404|Toondahra Granite|73450|4|Described|p4, p10, p22-23, p28, p36-37|Norian|Norian|Defined by Withnall (1972). Crops out as scattered boulders and pavements and forms an irregular, NE-aligned intrusion south of Mundubbera. A much smaller area of cream, locally flow-banded, very fine-grained, finely porphyritic leucogranite exposed farther south is delineated as subunit 'f' and a discrete pluton of relatively fresh hornblende-biotite tonalite as subunit 't' (Cranfield et al., 2001). Scattered miarolitic cavities up to ca 1 cm across common. K-Ar date of 215 +/- 6 Ma. Cut by numerous rhyolite dykes.|215 +/- 6 Ma K-Ar|||Intrudes Wandilla Formation, Dunollie beds and Munboorie beds?, Rockhampton Group, Boondooma and Wilfred Creek Igneous Complexes, and Arangbanga Volcanic Group.|Pale pink-pink or pale greenish grey, fine to coarse-grained, partly granophyric syenogranite to alkali feldspar granite that is variably altered.|
18415|Toowoomba Volcanics|23799|5|Briefly described|p54, p55|Tertiary|Tertiary|Of the Main Range Volcanics.  Geological Province: Main Range-Lamington Volcanic Province.||||||
18415|Toowoomba Volcanics|31132|6|Mentioned|p148|||Refers Webb et al. (1967)||||||
18415|Toowoomba Volcanics|34507|5|Briefly described|p87|||||||||
18415|Toowoomba Volcanics|39445|5|Briefly described|Table 14|||||||||
18415|Toowoomba Volcanics|44786|14|Not recorded|p193-202||Miocene|Early Miocene.||||||
18415|Toowoomba Volcanics|45087|5|Briefly described|p166|||Chemical analyses.||||||
18423|Top Nettle Microgranite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite.||||||
18423|Top Nettle Microgranite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||
18423|Top Nettle Microgranite|41297|6|Mentioned|Fig.1|||||||||
18423|Top Nettle Microgranite|60425|4|Described|p284-5 Appdx.|Late Carboniferous|Late Carboniferous|Of Go Sam Suite (O'Briens Creek Supersuite). Informally referred to as Top Nettle porphyry. Porphyritic biotite microgranite. I-type.||||||07-FEB-11
18425|Top Rocky Rhyolite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1725+/-3Ma.||||||12-DEC-06
18425|Top Rocky Rhyolite|23398|4|Described|p437|Statherian|Statherian|Age: 1725+/-3Ma.||||||12-DEC-06
18425|Top Rocky Rhyolite|24442|5|Briefly described|p22 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Carrara Range Group.  Geological Province: McArthur Basin.  See also p23 Fig. 2.||||||07-NOV-08
18425|Top Rocky Rhyolite|38237|6|Mentioned|p126|||||||||
18425|Top Rocky Rhyolite|39338|5|Briefly described|p352|||||||||
18425|Top Rocky Rhyolite|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Carrara Range Group.  Massive reddish-brown feldspar porphyry, probably rhyolite; minor basalt or trachyte.  Unconformably overlies Mitchiebo Volcanics; unconformably overlain by Musselbrook Formation (McNamara Group).||||||12-DEC-06
18425|Top Rocky Rhyolite|39497|4|Described|p10|||||||||
18425|Top Rocky Rhyolite|39925|6|Mentioned|p331|||See also p337.||||||12-DEC-06
18425|Top Rocky Rhyolite|40811|6|Mentioned|p318|||||||||
18425|Top Rocky Rhyolite|45166|5|Briefly described|p27|||||||||
18425|Top Rocky Rhyolite|49018|2|Defined|p5|Carpentarian|Carpentarian|||||||
18425|Top Rocky Rhyolite|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. Pink, porphyritic, massive to flow banded, spherulitic to microgranophyric rhyolite; local autobreccia, peperite and hyaloclastite.||||||
18425|Top Rocky Rhyolite|63109|6|Mentioned|p1109|||||||||
18425|Top Rocky Rhyolite|63866|5|Briefly described|p57|Statherian|Statherian|Carrara Range, Leichhardt Superbasin.|1725 +/- 3 Ma (Page et al., 2000)|||Overlies the Michiebo Volcanics. Possibly equivalent to the Eastern Creek Volcanics.||
18425|Top Rocky Rhyolite|65337|3|Fully described|p6 Fig.3, p10 Table 3, pp14-16. |||Thickness to 400 m of moderate-aspect-ratio lava flow(s) and marginal ephemeral alluvial and debris flows. Described in detail.|1725 +/- 3 Ma (Page et al. 2000).|Unit in Carrara Range Group.||Overlies Gator Sandstone. Is unconformably overlain by Surprise Creek Formation and, locally, by Bullrush Conglomerate.|Lower part: pink, quartz and K-feldspar porphyritic, massive to flow banded, spherulitic to microgranophyric rhyolite; local autobreccia, peperite and hyaloclastite. Upper part: poorly-sorted matrix-supported pebble to boulder conglomerate.|
18425|Top Rocky Rhyolite|69433|4|Described|p18:2, 6-9|Statherian|Statherian|Southern succession, Lawn Hill Platform. Up to 400m thick. SHRIMP U-Pb zircon age.|1725 +/- 3 Ma (Page et al., 2000).|Carrara Range Group.||Unconformably overlies Gator Sandstone and locally the Mitchiebo Volcanics. Is overlain unconformably by Surprise Creek Volcanics or Bullrush Conglomerate.|Coherent porphyritic rhyolite, overlain by matrix-supported conglomerate, with subangular to subrounded, locally imbricated clasts set in a pink lithic gravel-sand-mud matrix, and crudely horizontally stratified and ungraded.|12-JUL-16
18425|Top Rocky Rhyolite|69673|4|Described|p52 fig 42,|Statherian|Statherian|Up to 400m thick.|1725 +/- 3 Ma|Carrara Range Group|||Rhyolite overlain by matrix supported conglomerate with imbricated clasts set in a gravel-sand-mud matrix.|
18425|Top Rocky Rhyolite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1725+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
18425|Top Rocky Rhyolite|72526|5|Briefly described|p8 Fig.1.3.|Paleoproterozoic|Paleoproterozoic|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon igneous crystallisation age.|1725 +/-3 Ma|Carrara Range Group||Overlies Gator Sandstone and shown as underlying Fiery Creek Volcanics and Bigie Formation.||
18425|Top Rocky Rhyolite|72527|4|Described|p7, 87, 89, p119-120, p127-129, 194,196|Paleoproterozoic|Paleoproterozoic|One of three units considered to represent c. 1725 Ma felsic volcanism in the region, including Peters Creek Volcanics and Hobblechain Volcanics. Provides maximum age for overlying Bullrush Conglomerate.  See also p147-148, p154.|1725 +/- 3 Ma (Page et al 2000)|Top of Carrara Range Group||Unconformably overlies Gator Sandstone, unconformably underlies Surprise Creek Formation, Bullrush Conglomerate, and is laterally equivalent to Peters Creek Volcanics.||
18425|Top Rocky Rhyolite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the East part of the South Nicholson Basin and the Lawn Hill Platform. U-Pb zircon igneous crystallisation age shown.|1725 +/- 3 Ma|Carrara Range Group||Overlies Gator Sandstone and is shown as unconformably underlying Fiery Creek Volcanics and Bigie Formation.||
18425|Top Rocky Rhyolite|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Unconformably underlain by Gator Sandstone. Unconformably overlain by Surprise Creek Formation.||
18425|Top Rocky Rhyolite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1725 +/- 3 Ma (see Fig.1.2)|Carrara Range Group||Underlain by Gator Sandstone. Unconformably overlain by Surprise Creek Formation*.||
18425|Top Rocky Rhyolite|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|Age determination from Page et al. (2000).|1725 +/- 3 Ma|||||
18438|Torpedo Creek Quartzite|22438|4|Described|p539, Fig.3 p537|||See also Fig.10a p546.||||||12-DEC-06
18438|Torpedo Creek Quartzite|22453|6|Mentioned|p 11|||||||||
18438|Torpedo Creek Quartzite|22585|6|Mentioned|Fig3 P738|||Actually spelt Torpedo Creek Qtz.||||||
18438|Torpedo Creek Quartzite|22680|6|Mentioned|85,86|||Of McNamara Group. Overlies Kamarga Volcanics, Yeldham Granite and Surprise Creek Formation.||||||
18438|Torpedo Creek Quartzite|23031|6|Mentioned|24|||Geological  province: Lawn Hill Subprovince. Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23073|5|Briefly described|p744 (Fig 2)|||||||||
18438|Torpedo Creek Quartzite|23198|6|Mentioned|p873|||||||||
18438|Torpedo Creek Quartzite|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
18438|Torpedo Creek Quartzite|23393|4|Described|p18, p19|Paleoproterozoic|Paleoproterozoic|Of MacNamara Group. Overlain by Gunpowder Creek Formation.||||||07-NOV-08
18438|Torpedo Creek Quartzite|23396|5|Briefly described|p407 Fig.2|||Of the  McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23397|5|Briefly described|p463|||Of the Mount Isa Group (?).||||||12-DEC-06
18438|Torpedo Creek Quartzite|23398|5|Briefly described|p447|||Of McNamara Group.||||||
18438|Torpedo Creek Quartzite|23399|4|Described|p493|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|23406|6|Mentioned|p618|||Mentioned in terms of equivalents and correlatives.||||||
18438|Torpedo Creek Quartzite|23408|4|Described|p513 Fig. 2, p514, p15|||Of the  McNamara Group. Overlies Myally Subgroup.||||||15-JUN-09
18438|Torpedo Creek Quartzite|23466|5|Briefly described|p273|||||||||
18438|Torpedo Creek Quartzite|23518|4|Described|p12|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Western Fold Belt.||||||
18438|Torpedo Creek Quartzite|23767|5|Briefly described|p1956 Fig. 2|||Geological Province: Western Fold Belt. See also p1957 Fig.3.||||||
18438|Torpedo Creek Quartzite|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
18438|Torpedo Creek Quartzite|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
18438|Torpedo Creek Quartzite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group. Geological Province:  Mount Isa Superbasin||||||07-NOV-08
18438|Torpedo Creek Quartzite|24419|5|Briefly described|p16-17|Paleoproterozoic|Paleoproterozoic|Thin, widespread sandstone unit - polymictic conglomerate grading upwards into cross-bedded quartzose to feldspathic sandstone, siltstone and shale.  Conformably overlain by, and interfingers with Gunpowder Creek Fm.  Part of the Prize Supersequence.||||||26-FEB-18
18438|Torpedo Creek Quartzite|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Overlies Surprise Creek Formation.||||||
18438|Torpedo Creek Quartzite|30535|6|Mentioned|p403|||Refers Cavaney (1975).||||||12-DEC-06
18438|Torpedo Creek Quartzite|37459|2|Defined|p427|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||01-OCT-08
18438|Torpedo Creek Quartzite|37568|5|Briefly described|p84|||||||||
18438|Torpedo Creek Quartzite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|38232|6|Mentioned|p87|||||||||
18438|Torpedo Creek Quartzite|38237|4|Described|p127|||||||||
18438|Torpedo Creek Quartzite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|38348|4|Described|p8|||||||||
18438|Torpedo Creek Quartzite|38350|4|Described|p15|||||||||
18438|Torpedo Creek Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18438|Torpedo Creek Quartzite|39445|5|Briefly described|Table 2|||See also p35.||||||12-DEC-06
18438|Torpedo Creek Quartzite|39497|6|Mentioned|Fig.4|||||||||
18438|Torpedo Creek Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  White medium orthoquartzite with gypsum pseudomorphs locally. Overlies the Surprise Formation; underlies the Gunpowder Creek Formation.||||||15-JUN-06
18438|Torpedo Creek Quartzite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|39925|6|Mentioned|Fig.9|||||||||
18438|Torpedo Creek Quartzite|39944|3|Fully described|p229|||||||||
18438|Torpedo Creek Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18438|Torpedo Creek Quartzite|40221|3|Fully described|p13|||||||||
18438|Torpedo Creek Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
18438|Torpedo Creek Quartzite|41307|4|Described|p16|||||||||
18438|Torpedo Creek Quartzite|42367|5|Briefly described|p18|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|43235|5|Briefly described|p9,Fig.10.|||Of the McNamara Group.||||||12-DEC-06
18438|Torpedo Creek Quartzite|45161|5|Briefly described|Table 3|||||||||
18438|Torpedo Creek Quartzite|45166|5|Briefly described|p30|||||||||
18438|Torpedo Creek Quartzite|47083|3|Fully described|p14||Proterozoic|Previously included in Mammoth Formation. Of McNamara Gp. O'lying unit Gunpowder Crk Fm. U'lying unit Surprise Crk Fm. Maximum thickness 300 m.||||||
18438|Torpedo Creek Quartzite|49041|6|Mentioned|Table 4|||||||||
18438|Torpedo Creek Quartzite|50550|5|Briefly described|p1139 Fig.2||Statherian|Conformably overlies Surprise Creek Formation. Overlain by Gunpowder Creek Formation at a syn-rift unconformity. Geological Province: Western Fold Belt
.||||||20-JUN-22
18438|Torpedo Creek Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the McNamara Group. Meta-arenite, quartzite; minor conglomerate.||||||
18438|Torpedo Creek Quartzite|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||23-FEB-20
18438|Torpedo Creek Quartzite|62535|5|Briefly described|p672|Statherian|Statherian|Lawn Hill Platform. Lithology not specified.||McNamara Group.||||
18438|Torpedo Creek Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone.||||||30-SEP-08
18438|Torpedo Creek Quartzite|63111|5|Briefly described|p1163 Fig. 3, p1171|Statherian|Statherian|Of Gun Supesequence. Age: ~ 1690+/-7Ma.  Geological Province: Calvert Superbasin. Consists of sandstone.||||||07-FEB-11
18438|Torpedo Creek Quartzite|63113|6|Mentioned|p1214 Fig.2, p1225 Fig.13. |||Part of Prize and Gun supersequences. Appears in Fig.2 only as Torp.|1659 Ma.|Of the McNamara Group||||
18438|Torpedo Creek Quartzite|63114|5|Briefly described|p1253 Fig.2. |||Appears only as Torpedo.||||||
18438|Torpedo Creek Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Calvert and Isa superbasins.||||||
18438|Torpedo Creek Quartzite|63116|6|Mentioned|p1297 Fig.2, |||Calvert and Isa superbasins. Material properties detailed.||||||
18438|Torpedo Creek Quartzite|64250|6|Mentioned|p11 fig.3|||Western Fold Belt, Mount Isa Inlier.||||Overlies Surprise Creek Formation. Is overlain by Lower Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin. Only shown as Torpedo in Fig.2.|||||Sandstone.|
18438|Torpedo Creek Quartzite|65337|5|Briefly described|p5, p33 Fig.27.|||Calvert Superbasin.||Unit in McNamara Group.||Overlies Surprise Creek Formation. Is overlain by Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|65396|6|Mentioned|p82, p175, p241|||Calvert Superbasin. Cover Sequence 2. Lawn Hill Platform.||||Overlies Surprise Creek Formation; overlain by Lower Gunpowder Creek Formation||
18438|Torpedo Creek Quartzite|66844|5|Briefly described|p264-265,270|||Lawn Hill Platform. See also Torpedo Creek Formation [Names used interchangeably]. Abrupt thickness variations imply highly localised sediment sources and discrete depocentres.||Of lower McNamara Group; Prize Supersequence.||Basal unit within the Prize Supersequence. Overlain by lower Gunpowder Creek Formation.|Nonmarine and nearshore sandstone.|
18438|Torpedo Creek Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p34|Paleoproterozoic|Paleoproterozoic|Century and Mount Oxide Domains, Mount Isa Inlier. Isa (Calvert) Superbasin. See also reference to Torpedo Creek Formation (Mount Isa Block Time-Space Plot).|~1690-1670 Ma.|McNamara Group.|||White to medium orthoquartzite, with gypsum pseudomorphs locally.|
18438|Torpedo Creek Quartzite|68146|5|Briefly described|p84, p189, p199-200|||Mentioned in exactly the same context as Torpedo Creek Formation (p3, p86).||||Overlies Fiery Creek Volcanics. Lateral equivalent to Warrina Park Quartzite.||02-NOV-18
18438|Torpedo Creek Quartzite|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlain by Gunpowder Creek Formation||
18438|Torpedo Creek Quartzite|68575|4|Described|p3, p6-7, p40, p52-60, p125, p127, p134|||Mount Isa Region. Other age determinations discussed: the authors favour 1697 +/- 12 Ma by Neumann et al. (2009). Has a provenance (detrital zircon populations) significantly different from Saint-Smith and Bularnu Formations. Whole rock Sm-Nd isotopic data and age (1757 Ma).|1756 +/- 16 Ma (maximum depositional age).|||Overlies Big Toby Granite and Surprise Creek Formation. Is overlain by Gunpowder Formation.|Well-sorted, medium-grained metamorphosed and silicified feldspathic sandstone.|
18438|Torpedo Creek Quartzite|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier.||Lower McNamara Group.||Overlies Surprise Creek Beds. Is overlain by Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|68732|6|Mentioned|p160, p168 Fig.5|||Prize Supersequence.|||||Siliciclastic sediments.|01-DEC-17
18438|Torpedo Creek Quartzite|69591|4|Described|p38 Fig.2.22, p40, p42-44, p54, p107|||Mount Oxide and Leichhardt River Domains, Calvert Superbasin. Part of Prize and Gun Supersequences. Fluvial/shoreface deposits. These maximum depositional ages, by Neumann et al. (2009), are for lower and upper parts respectively.|1697 +/- 12 Ma and ~1674 +/- 6 Ma.|Basal McNamara Group.||Unconformably overlies Yeldham Granite. Is overlain by Gunpowder Creek Formation.|White to medium orthoquartzite, with gypsum pseudomorphs locally. Basal quartzite and conglomerate unit.|
18438|Torpedo Creek Quartzite|70864|5|Briefly described|p75||Paleoproterozoic|||Base of McNamara Group|||Sandstone and conglomerate.|
18438|Torpedo Creek Quartzite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1756+/-16 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
18438|Torpedo Creek Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown, with Warrina Park Quartzite, as located in the Lawn Hill Platform, Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province and the eastern part of the South Nicholson Basin.||||Overlies Surprise Creek Formation and partially underlies lower Gunpowder Creek Formation and is shown as unconformably underlying Mount Isa Group.||
18438|Torpedo Creek Quartzite|72912|5|Briefly described|p5 Fig.3, p13.|Statherian|Statherian|Of Calvert Superbasin. Located in the Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt and the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. Listed with Warrina Park Quartzite. Lateral equivalent? U-Pb zircon sedimentary depositional age of overlying 'lower Gunpowder Creek Formation' is 1694+/-3 Ma, and of underlying Surprise Creek Formation is 1688+/-5 Ma.||Of Prize supersequence.||Overlies Surprise Creek Formation and partially underlies Gunpowder Creek Formation, Lower. May unconformably underlie Moondarra Siltstone.||
18438|Torpedo Creek Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Listed as Torpedo Creek/Warrina Park Quartzite in Fig.1.2; does not specify / distinguish between the two units.||||Uncertain distinction from Warrina Park Quartzite. Underlain by Surprise Creek Formation. Partly overlain by lower Gunpowder Creek Formation.||
18438|Torpedo Creek Quartzite|73144|6|Mentioned|p10|||Said to be part of the Prize Supersequence. Written as Torpedo Creek quartzite. [c.f. Torpedo Creek Formation p9, shown as part of the Gun Supersequence]||||||17-OCT-22
18438|Torpedo Creek Quartzite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
18438|Torpedo Creek Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1697+/-12 Ma maximum depositional age||||Siliciclastics.|
18492|Towallum Basalt|22857|5|Briefly described|p319 Fig.22.10B, p548 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Vesicular tholeiitic basalt, volcaniclastics. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. See also p318-9.||||||
18492|Towallum Basalt|22865|5|Briefly described|p318,Table22.2p308||Early Jurassic|Max Age: 187 (+/-) 5 Ma.||||||
18492|Towallum Basalt|23720|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|of the Walloon Coal Measures.  Basalt, minor basalt breccia.||||||
18492|Towallum Basalt|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Koukandowie Formation. Maximum thickness: 50m.  Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|23843|5|Briefly described|p456 Table 1|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 15m.||||||
18492|Towallum Basalt|24127|5|Briefly described|p5|Jurassic|Jurassic|Max. thickness: 60m.||||||
18492|Towallum Basalt|24129|6|Mentioned|p4|||||||||
18492|Towallum Basalt|30785|6|Mentioned|p397|||||||||
18492|Towallum Basalt|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
18492|Towallum Basalt|34340|3|Fully described|p469|||||||||
18492|Towallum Basalt|34593|6|Mentioned|p539|||||||||
18492|Towallum Basalt|36570|6|Mentioned|p39|||||||||
18492|Towallum Basalt|37122|6|Mentioned|Table 1|||||||||
18492|Towallum Basalt|40245|6|Mentioned|p187|||||||||
18492|Towallum Basalt|42248|6|Mentioned|p405|||||||||
18492|Towallum Basalt|42925|6|Mentioned|p86|||||||||
18492|Towallum Basalt|43150|5|Briefly described|Map Legend||Jurassic|Of the Koukandowie Formation. Tholeiitic basalt at base in the south. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
18492|Towallum Basalt|43383|14|Not recorded|p24|Jurassic|Triassic|||||||
18492|Towallum Basalt|43479|14|Not recorded|p249,262|Late Jurassic|Middle Jurassic|||||||
18492|Towallum Basalt|43881|14|Not recorded|p6-7,11,37-8,49,52-3|Jurassic|Triassic|p59(anal.),62-3,133.||||||
18492|Towallum Basalt|44028|14|Not recorded|Fig.2||Jurassic|See Strat Table.||||||
18492|Towallum Basalt|44450|4|Described|p28 Table 7|Middle Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin. Max. thickness: >60 m.||||||
18492|Towallum Basalt|45003|14|Not recorded|p238|||||||||
18492|Towallum Basalt|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
18492|Towallum Basalt|60281|5|Briefly described|Fig.18 Appendix 1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation.  Vesicular basalt, volcaniclastics.  Max. thickness: 50m.||||||
18492|Towallum Basalt|60993|5|Briefly described|p8 Fig. 4|||Of the Marburg Subgroup. Overlain by Koukandowie Formation members, Ma Ma Creek Member and Heifer Creek Sandstone Member. Overlies Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60995|4|Described|p65, p51 Fig. 3|Early Jurassic|Early Jurassic|Originally designated as part of Marburg Fm overlying Koukandowie Sst Mbr; revised and now part of Marburg Subgrp, beneath Heifer Creek Sst Mbr (part of Koukandowie Fm?). Max. thickness: 50m. Geol. Prov: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60996|5|Briefly described|p113 Fig. 64|||Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60997|4|Described|p138|Toarcian|Pleinsbachian|Previously mapped as lying between the Marburg "Fm" and Walloon C.M with age 175-163Ma; now revised to age 187+/-10Ma lying between Gatton Sst and Heifer Creek Sst Mbr.  Max. thick: 15m. Geol. Prov: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Early Jurassic|Tholeiitic basalt. Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|61794|6|Mentioned|p355|||Olivine tholeiite.||||||
18492|Towallum Basalt|69297|5|Briefly described|p487 fig 5.38|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 10-50m thick. Deposited in a terrestrial or lacustrine environment.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Ma Ma Creek Member.|Vesicular basalt and volcaniclastics.|
18508|Towers Hill Granite|22847|3|Fully described|p 39|Ordovician|Early Ordovician|||||||
18508|Towers Hill Granite|23422|6|Mentioned|p209 Table 6.6|||||||||
18508|Towers Hill Granite|23423|5|Briefly described|p228||Ordovician|In the Ravenswood Batholith.||||||
18508|Towers Hill Granite|23513|5|Briefly described|Map legend||Ordovician|Palaeozoic Intrusive No. 462. I-Type.||||||
18508|Towers Hill Granite|42633|5|Briefly described|Table 1 P11|||Variation on Towers Hill Granodiorite||||||
18508|Towers Hill Granite|42750|2|Defined|p35|Middle Ordovician||||||||
18508|Towers Hill Granite|43093|4|Described|Appendix 1|Ordovician|Early Ordovician|Probable Early to Middle Ordivician||||||
18508|Towers Hill Granite|43259|4|Described|Appendix 1,p49.||Ordovician|||||||
18508|Towers Hill Granite|43934|5|Briefly described|Map Legend||Ordovician|||||||
18508|Towers Hill Granite|50552|5|Briefly described|p1048 Fig.2|Late Ordovician|Early Ordovician|Part of Ravenswood Batholith, Lolworth-Ravenswood Terrane.||||||
18508|Towers Hill Granite|60425|5|Briefly described|p11|Ordovician|Ordovician|Part of Ravenwood Batholith in Charters Towers region. I-type granite.||||||07-FEB-11
18508|Towers Hill Granite|62074|5|Briefly described|p2-3|Middle Ordovician|Middle Ordovician|Near Charters Towers. Only mildly deformed.||||Is intruded by Millchester Creek Tonalite.||
18508|Towers Hill Granite|62075|6|Mentioned|p11 Fig.3, p17|Middle Ordovician|Early Ordovician|Appears as Towers Hill granite. Charters Towers District. Auriferous splay fault-hosted veins occurred at the contact of this unit with the Washington diorite.||||||
18508|Towers Hill Granite|62521|5|Briefly described|p8, p26|Middle Ordovician|Late Cambrian|Of the Hogsflesh Creek Supersuite. Geological Province: Ravenswood Batholith. Grey to cream, medium-grained, even-grained biotite granite.||||||14-JAN-08
18508|Towers Hill Granite|68576|5|Briefly described|Q_11: p41-42|||Towers Hill, Charters Towers.|||||Fine- to medium-grained biotite granodiorite to granite; contains minor hornblende.|
18529|Train Range Ironstone Member|23393|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|Of Mullera Formation.||||||
18529|Train Range Ironstone Member|23937|5|Briefly described|p62|||Of the Mullera Formation (South Nicholson Group).  Geological Province: Roper Superbasin.  See also p93 Appendix 1.||||||
18529|Train Range Ironstone Member|24047|5|Briefly described|p27|||Equivalent to the Sherwin Formation.||||||
18529|Train Range Ironstone Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18529|Train Range Ironstone Member|38348|6|Mentioned|p24|||||||||
18529|Train Range Ironstone Member|39497|6|Mentioned|p15|||||||||
18529|Train Range Ironstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
18529|Train Range Ironstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Mullera Formation.||||||
18529|Train Range Ironstone Member|45166|5|Briefly described|p33|||||||||
18529|Train Range Ironstone Member|65337|5|Briefly described|p58.|||Several ironstone intervals in the lower Mullera Formation that were the focus of exploration: the Constance Range deposits. Mineralisation is due to primary depositional processes and local surficial supergene enrichment and fault-related fluid movement.||Unit in South Nicholson Group.|||Contains three or four ore-grade beds; mineralisation consists of oolitic hematite, siderite and chamosite beds: "Wabana type".|
18529|Train Range Ironstone Member|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Hematitic and limonitic sandstone; siderite and chamosite-rich at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|67539|6|Mentioned|p15, Fig.8|||||Of the Mullera Formation.||||
18529|Train Range Ironstone Member|68020|5|Briefly described|p128|||45-180m thick.||?Of Mullera Formation?|||Lenticular ironstone beds and thinly bedded alternating dark grey shales, siltstones and sandstones.|
18529|Train Range Ironstone Member|68146|6|Mentioned|p196|||||Mullera Formation||||02-NOV-18
18529|Train Range Ironstone Member|69434|5|Briefly described|p19:7|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960), Harms (1965), Slater and Mond (1980). Explored for iron in Qld: fourteen separate iron ore deposits identified.||Mullera Formation.|||Ironstone beds.|12-JUL-16
18529|Train Range Ironstone Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT).||Mullera Formation.|||Contains numerous low-grade to high-grade hematite/goethite/siderite deposits of the oolitic type.|
18529|Train Range Ironstone Member|70897|5|Briefly described|p39, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|Appears in Fig.1.7.6 as Train Range Fe. Described as member of South Nicholson Group p39. Diagram suggests is a member of the Mullera Formation.||Mullera Formation.||Identical with Sherwin Ironstone Member (Roper Group).|Shallow-water oolitic ironstone.|28-NOV-17
18529|Train Range Ironstone Member|71369|4|Described|p1, p5-6, p33, p37-42, p44, p50|Mesoproterozoic|Mesoproterozoic|Initially named and defined as Train Range iron-bearing member by Carter and Zimmerman (1960) [actually their name was the more formal Train Range Iron-bearing Member]. Later the Train Range Ironstone Formation of Harms (1965). Modified to Train Range Ironstone Member by Slater and Mond (1980) and Sweet and Hutton (1982), who saw it as better included within the Mullera Formation than as a separate Formation. South Nicholson Basin. 45-180m thick. Progradational deposits.||Mullera Formation.|||Comprises a series of ferruginous sandstone and ironstone beds which are laterally gradational. Ironstones are largely oolitic at depth.|20-FEB-18
18529|Train Range Ironstone Member|72297|5|Briefly described|p712|||Constance Range area west of Lawn Hill; South Nicholson Basin.||South Nicholson Group.|||Up to ten lenticular beds of oolitic iron formation, interbedded with shale, siltstone and sandstone.|
18529|Train Range Ironstone Member|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72416|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds.|
18529|Train Range Ironstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.||Unit of Mullera Formation.|||Hematitic and limonitic sandstone; hematitic, sideritic and chamosite-rich oolites at depth; siltstone and shale interbeds|
18529|Train Range Ironstone Member|72912|4|Described|p5 Fig.3, p23, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin. Name shown in full p23, but mostly abbreviated to Train Range Ironstone.||Mullera Formation||||
18529|Train Range Ironstone Member|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||Mullera Formation, Accident Subgroup, South Nicholson Group||||
18558|Traveston Formation|24078|5|Briefly described|p425 Tb. 1|Early Triassic|Early Triassic|Thinly bedded, olive green shales.  Max. thickness: 820m.  Geological Province: Gympie Basin.||||||
18558|Traveston Formation|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
18558|Traveston Formation|30655|6|Mentioned|p12|||Refers Runnegar & Fergusson (1969)||||||
18558|Traveston Formation|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
18558|Traveston Formation|33168|6|Mentioned|p121|||Refers Runnegar (1969)||||||
18558|Traveston Formation|34474|6|Mentioned|Fig.1|||Lower Triassic||||||
18558|Traveston Formation|34475|2|Defined|p269|Early Triassic|Early Triassic|M. & L.Triassic||||||
18558|Traveston Formation|35101|6|Mentioned|p33|||||||||
18558|Traveston Formation|36045|6|Mentioned|p334|||||||||
18558|Traveston Formation|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
18558|Traveston Formation|39284|5|Briefly described|p431|||||||||
18558|Traveston Formation|41157|6|Mentioned|Fig.1|||||||||
18558|Traveston Formation|42450|5|Briefly described|p405|||||||||
18558|Traveston Formation|43008|5|Briefly described|map legend|||||||||
18558|Traveston Formation|43017|5|Briefly described|Fig.3,p375|||||||||
18558|Traveston Formation|43100|6|Mentioned|p33|||||||||
18558|Traveston Formation|65380|5|Briefly described|p671|Early Triassic|Early Triassic|Age: middle Early Triassic, from ammonites.||||Overlies Keefton Formation.||27-MAR-12
18558|Traveston Formation|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Gympie Province. This unit, as well as the Brooweena and Keefton Formations, and the Kin Kin beds, are all mapped under the symbol, Rb.||||||
18558|Traveston Formation|68679|5|Briefly described|p312-313, p369|Triassic|Triassic|Runnegar and Ferguson (1969). Northern New England Orogen. Murphy et al. (1976) combined this unit with the Kin Kin Phyllite, which were not possible on field relationships to map separately, into the Kin Kin beds.||Gympie Group.||||
18594|Trimble Member|23425|4|Described|Table 9.7 p394.||Albian|Of Rolling Downs Group. Geological Province Carpentaria Basin.||||||
18594|Trimble Member|23496|5|Briefly described|Table 4, p59||Aptian|of Woods 1961, then Smart and Others 1972. of Wallumbilla Formation, Rolling Downs Group. ~68m thick.||||||
18594|Trimble Member|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Of Wallumbilla Formation. Supersedes Trimble Formation.  Maximum thickness: 70m.  Geological Province: Carpentaria Basin.||||||
18594|Trimble Member|31168|5|Briefly described|p11|||See also Table 2.||||||
18594|Trimble Member|33179|4|Described|p11|||||||||
18594|Trimble Member|33182|6|Mentioned|Fig.1|||||||||
18594|Trimble Member|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18594|Trimble Member|37608|3|Fully described|Table 2|||||||||
18594|Trimble Member|39211|5|Briefly described|p36|||See Fig. 22||||||
18594|Trimble Member|43287|5|Briefly described|Map Legend||Early Cretaceous|||||||
18594|Trimble Member|43630|6|Mentioned|Fig.4,p7|||fig.4||||||
18594|Trimble Member|45145|3|Fully described|Table 5|||||||||
18594|Trimble Member|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Wallumbilla Formation (Rolling Downs Group). Mudstone, labile sandstone; minor limestone.||||||
18594|Trimble Member|69594|5|Briefly described|p522|Early Cretaceous|Early Cretaceous|Woods (1961); Smart et al. (1980). Weipa Sub-basin, Carpentaria Basin. A local, probably early Albian unit. Up to 70m thick.||Wallumbilla Formation.|||Siltstone, limestone and glauconitic lithic sandstone.|
18633|Tuckers Igneous Complex|22847|3|Fully described|p 59|Early Permian||||||||
18633|Tuckers Igneous Complex|23049|6|Mentioned|p63|||||||||
18633|Tuckers Igneous Complex|23422|5|Briefly described|p218 Table 6.12|||Of Tuckers Suite.||||||
18633|Tuckers Igneous Complex|23504|5|Briefly described|Map Legend||Permian|||||||
18633|Tuckers Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 189. I-Type.||||||
18633|Tuckers Igneous Complex|23617|5|Briefly described|p30|||||||||
18633|Tuckers Igneous Complex|23893|6|Mentioned|p13|||||||||
18633|Tuckers Igneous Complex|24334|5|Briefly described|p48 Tb.1|Early Permian|Early Permian|Age: 284 - 291 Ma.||||||
18633|Tuckers Igneous Complex|24424|5|Briefly described|p523|Early Permian|Early Permian|Age: c. 286+/-6 Ma. Diorite, gabbro, monzodiorite and granodiorite. Palaeomagnetism described.||||||04-FEB-05
18633|Tuckers Igneous Complex|30148|4|Described|p24|||Upper Carboniferous - Lower Permian age.4 phase. See also p25-28.||||||13-MAR-19
18633|Tuckers Igneous Complex|30149|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous to Lower Permian age||||||
18633|Tuckers Igneous Complex|30151|4|Described|Table 2|||277-282 m.y. Upper Carboniferous to Lower Permian age.||||||
18633|Tuckers Igneous Complex|30914|6|Mentioned|Map legend|Permian|Permian|||||||
18633|Tuckers Igneous Complex|31813|6|Mentioned|Table 2|||Carb. - Permian||||||
18633|Tuckers Igneous Complex|32553|4|Described|p66|||||||||
18633|Tuckers Igneous Complex|34409|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Upper Carboniferous - Lower Permian||||||
18633|Tuckers Igneous Complex|34573|6|Mentioned|p31|||See also PP32,37. 280my||||||
18633|Tuckers Igneous Complex|36472|6|Mentioned|Map legend|Early Permian|Late Carboniferous|Early Permian to Late Carboniferous||||||
18633|Tuckers Igneous Complex|37613|6|Mentioned|Fig.3|||||||||
18633|Tuckers Igneous Complex|39445|5|Briefly described|Table 12|||||||||
18633|Tuckers Igneous Complex|39734|6|Mentioned|p21|||||||||
18633|Tuckers Igneous Complex|42245|6|Mentioned|p37|||||||||
18633|Tuckers Igneous Complex|43093|4|Described|Appendix 1|||K-Ar dates of 283+/-9Ma & 288+/-9Ma.||||||
18633|Tuckers Igneous Complex|43259|4|Described|Appendix 1,p28.|Permian|Carboniferous|K-Ar age is 280+/-8 Ma.||||||
18633|Tuckers Igneous Complex|43936|5|Briefly described|Map Legend||Permian|||||||
18633|Tuckers Igneous Complex|45151|5|Briefly described|Table 7|||||||||
18633|Tuckers Igneous Complex|48914|2|Defined|p82|Permian|Carboniferous|Carboniferous - Permian - New name||||||
18633|Tuckers Igneous Complex|62521|5|Briefly described|p38|Early Permian|Middle Ordovician|Mafic rocks. Geological Province: Ravenswood Batholith||||||14-JAN-08
18633|Tuckers Igneous Complex|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Permian|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|283-291 Ma magnetic age range|||||10-AUG-15
18662|Tully Granite Complex|23423|4|Described|p313 Table 7.4, p253|Early Permian|Late Carboniferous|Age: 286 +/- 4 Ma (SHRIMP), 273-302 Ma (K-Ar). Intrudes Hodgkinson Formation, Glen Gordon Volcanics. Overlain by Atherton Basalt (unconformable). In the Tully Batholith.||||||06-AUG-08
18662|Tully Granite Complex|23497|4|Described|Table 1||Permian|of Kennedy Province. Age: 286+/-4Ma(SHRIMP). Intrudes Hodgkinson Formation rocks and Glen Gordon Volcanics. Unconformably overlain by Atherton Basalt. Part of the I-type Ingham Supersuite.||||||
18662|Tully Granite Complex|23507|5|Briefly described|Map Legend||Early Permian|Age: 286+/-4Ma SHRIMP.||||||
18662|Tully Granite Complex|30505|5|Briefly described|p5|||See also P6,7. Permian age||||||
18662|Tully Granite Complex|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
18662|Tully Granite Complex|36563|6|Mentioned|Table 1|||||||||
18662|Tully Granite Complex|39445|5|Briefly described|Table 12|||||||||
18662|Tully Granite Complex|43259|4|Described|Appendix 1,p44.|Permian|Carboniferous|||||||
18662|Tully Granite Complex|43896|14|Not recorded|Map Legend||Permian|||||||
18662|Tully Granite Complex|43903|14|Not recorded|Map Legend||Early Permian|Early Permian to Middle (?) Carboniferous||||||
18662|Tully Granite Complex|43926|14|Not recorded|p17,Tb.2,opp.p10|||||||||
18662|Tully Granite Complex|43927|2|Defined|p11-25|||||||||
18662|Tully Granite Complex|44258|14|Not recorded|p40|||Intrudes Barron River Metamorphics.||||||
18662|Tully Granite Complex|45025|4|Described|p76||Permian|||||||
18662|Tully Granite Complex|45113|3|Fully described|p20|||Emphasis on petrography.||||||
18662|Tully Granite Complex|46845|6|Mentioned|Table 1|||||||||
18662|Tully Granite Complex|60425|3|Fully described|p58 Tb. 4, p100-101|Early Permian|Early Permian|Part of Tully Batholith and Ingham Supersuite. Age: 286+/-4Ma (SHRIMP), 273-3-2Ma (K-Ar). Quartz gabbro to biotite granite - mainly hornblende-biotite granite to biotite-hornblende granodiorite; clino- and ortho-pyroxene present in more mafic units.||||||07-FEB-11
18662|Tully Granite Complex|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|||||I-type granitoids.|
18662|Tully Granite Complex|69593|5|Briefly described|p495, p512|Permian|Early Carboniferous|Tully Batholith. Sm-Nd isotope data tabulated.|286 +/- 4 Ma.||||Mainly hornblende-biotite granite to (pyroxene-)biotite-hornblende granodiorite; ranges from biotite granite to quartz gabbro. I-type.|
18662|Tully Granite Complex|73450|6|Mentioned|p105|||||||||
18773|Ukalunda Formation|42547|5|Briefly described|Fig.17 P61|||Variation on Ukalunda beds.||||||
18773|Ukalunda Formation|68553|6|Mentioned|Map legend|Devonian|Devonian|This unit, as well as the Sedgeford Formation, the Douglas Creek Limestone, the Theresa Creek and Dunstable Volcanics, and unnamed Devonian sedimentary and volcanic units, are all mapped under the symbol, Da.||||||
18773|Ukalunda Formation|68679|6|Mentioned|p364|Devonian|Devonian|Thomson Orogen.||||||
18773|Ukalunda Formation|68731|5|Briefly described|p120, p171, p172, p177 Fig 3.91, p192|Early Devonian|Early Devonian|Previously assigned to the Ukalunda beds by Malone et al (1966). Now mapped in six main areas in BOWEN in addition to several small areas in MOUNT COOLON. < 1500 m thick.||||Underlain by the Anakie Metamorphic Group. Unconformably underlain by the the Les Jumelles beds. Disconformably overlain by the Mount Wyatt Formation.|Comprises fine- to medium-grained, labile to sublabile, lithic and feldspathic sandstone, mudstone and minor conglomerate and limestone.|
18773|Ukalunda Formation|68900|3|Fully described|p1-p2, p4-p5, p15, p22-p32|Devonian|Devonian|New name replacing the Ukalunda beds as the top and bottom of the unit has been identified thus justifying raising the unit to formation level. Named for Ukalunda homestead at 512900 7689000. Relatively undefomred, underlies Drummond Basin rocks. Outcrops in six main areas [provided in text]. No type section has been found as outcrop is generally poor, several areas contain partial sections and two are listed as reference sections [provided in text on p23]. Total thickness estimated at 1500m assuming no fold or fault repetition. Lithology and structure are discussed in some detail. Equivalent to the Douglas Creek Limestone.  Intruded by the Percy Douglas Granodiorite, the Sunbeam Granodiorite and Joe-de-Little Granodiorite.||||Overlies the Anakie Metamorphic Group and Les Jumelles beds. Overlain by the Mount Wyatt Formation.|Thick- to very thick-bedded, clast-supported, quartz-pebble conglomerate, mudstone, pebbly sandstone and sporadic limestone.|
18773|Ukalunda Formation|68901|6|Mentioned|p2 Fig. i|Devonian|Devonian|||||||27-SEP-18
18773|Ukalunda Formation|69541|5|Briefly described|p645 Fig.1(b), p654|Middle Devonian|Early Devonian|Thomson Orogen. Ukalunda Shelf, draping or bordering the Anakie Inlier.|||||Shallow-water sandstones and mudstones; less common conglomerate and fossil-rich limestone.|
18773|Ukalunda Formation|69592|6|Mentioned|p229|Devonian|Devonian|Scattered remnants in central QLD, developed on Thomson Orogen basement.||||||
18773|Ukalunda Formation|69952|5|Briefly described|p85, p108|Early Devonian|Early Devonian|Thomson Orogen.||||Overlies Les Jumelles beds.||
18773|Ukalunda Formation|70740|4|Described|i, ii, p1, p9, p18, p20, p23-p34, |Emsian|Emsian|Drummond Basin, Anakie Inlier. Defined as basement in the Drummond Basin. Name derived from the Ukalunda Homestead. Age derived from brachiopod fossils. Two reference sections are given and briefly described on p23-p24. Estimated to be between 900 to 1500m thick. Lithology, petrography, structure, fossil assemblage and regional context are discussed. Also overlain disconformably by Bulgonunna Volcanic Group. Intruded by Mount Magnus, Joe-De-Little, House and Kitchen, Peak John Well, and Roscow granites, the Sunbeam Granodiorite, Percy Douglas Tonalite and Wynne Creek Diorite. See also p36, p43, p44, p47, p51, p55, p72, p86, p88, p105, p127-p130.||||Unconformably overlies the Les Jumelles beds and the Anakie Metamorphic Group. Unconformably overlain by the Mount Wyatt Formation and the Bimurra Volcanics.|Basal conglomerate, grey mudstone, fossiliferous lithic sandstone, siltstone and impure limestone.|
18773|Ukalunda Formation|73035|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Some polygons of this unit are uncertainly identifed.|||||Shale, siltstone, medium to coarse-grained feldspathic sandstone, polymictic granule conglomerate, oligomictic.|
18781|Ulam Marble|31659|6|Mentioned|p28|||Refers Richards (1918)||||||
18781|Ulam Marble|68576|5|Briefly described|QLD_D1: p6, p10, p17|||Rockhampton. Used in the main dining room in Tattersall's Club, Brisbane; floors and panels in The Residences. Appears as Ulam marble in p6 and p10. Map location.|||||Strongly-textured marble.|
18819|Unbunmaroo Member|22954|4|Described|Fig1p6,17-9,21|Datsonian|Payntonian|||||||
18819|Unbunmaroo Member|36217|6|Mentioned|p206|||Published by Druce 1978. Definition approved by Qld SNC.||||||
18819|Unbunmaroo Member|37572|5|Briefly described|p161|||||||||
18819|Unbunmaroo Member|38532|4|Described|p242|||||||||
18819|Unbunmaroo Member|40136|5|Briefly described|p41|||||||||
18819|Unbunmaroo Member|40810|5|Briefly described|p14|||||||||
18819|Unbunmaroo Member|42354|6|Mentioned|p11|||Of Ninmaroo Formation.||||||13-DEC-06
18819|Unbunmaroo Member|46897|6|Mentioned|Fig.2|||||||||
18819|Unbunmaroo Member|46958|6|Mentioned|p195|||||||||
18819|Unbunmaroo Member|50244|6|Mentioned|p89 Fig. 1, p100 Fig. 7|Ordovician|Cambrian|Of Ninmaroo Formation. Geological Province: Georgina Basin.||||||22-APR-09
18819|Unbunmaroo Member|62793|6|Mentioned|p272|Late Cambrian|Late Cambrian|Contains latest Cambrian index species Cordylodus proavus. In Black Mountain section, C. proavus Assemblage Zone (lower Datsonian) is now defined as occurring between 130 m  and 230 m above the base of the Unbunmaroo Member.||Unit of Ninmaroo Formation.||||21-MAR-12
18819|Unbunmaroo Member|64068|4|Described|p73-74|Late Cambrian|Late Cambrian|Thickness 165 m in type section. Diverse fauna.||Base of Ninmaroo Formation.||Conformably to disconformably overlies Chatsworth Limestone. Is overlain by Jiggamore Member.|Peloid, ooid, peloid-intraclast and quartzic peloid grainstone, stromatolite boundstone, calcimudstone with evaporites.|05-APR-12
18819|Unbunmaroo Member|67323|5|Briefly described|GIS attrib tbl|Early Ordovician|Late Cambrian|Georgina Basin.||Cockroach Group|||Medium- to thick-bedded limestone (intraclast and peloid grainstone, mudstone, stromatolitic boundstone), dolomite, calcareous siltstone.|
18819|Unbunmaroo Member|71284|5|Briefly described|p489|||Black Mountain area, western Queensland. Contains the conodont Cordylodus proavus, which had been used to mark the base of the Ordovician in Australia.||Ninmaroo Formation.||||
18824|Undara Basalt|23291|4|Described|p80 Tb. 3.6|Pleistocene|Pleistocene|Parent: McBride Group. Age: 0.19Ma. Geological Province: Georgetown Region.||||||08-JUL-15
18824|Undara Basalt|23502|5|Briefly described|Map Legend||Quaternary|of McBride Basalt Group.||||||
18824|Undara Basalt|23510|5|Briefly described|Map Legend|Quaternary|Tertiary|||||||
18824|Undara Basalt|23616|5|Briefly described|Table 1B p11, p41||Cenozoic|Age: Pleistocene (0.19 Ma - Griffin & McDougall 1975). Unconformably overlies older basalts of McBride Basalt Group. Of McBride Basalt Group. McBride Basalt Province.||||||19-NOV-08
18824|Undara Basalt|23619|4|Described|p28 table 1||Pleistocene|Also see p13. Olivine basalt. Of the McBride Basalt Group in the McBride Basalt Province.||||||
18824|Undara Basalt|23624|4|Described|p28|||Geological Province: McBride Province.||||||08-JUL-15
18824|Undara Basalt|34046|6|Mentioned|Table III|||||||||
18824|Undara Basalt|41680|6|Mentioned|p106|||||||||
18824|Undara Basalt|42691|5|Briefly described|map legend|Cenozoic||||||||19-NOV-08
18824|Undara Basalt|43060|4|Described|p64,Table 1b|||see also Table 1c. Of McBride Basalt Group||||||
18824|Undara Basalt|43110|5|Briefly described|Table 5,p63.|||||||||
18824|Undara Basalt|43113|4|Described|Table 1 p16|||of McBride Basalt Group.||||||
18824|Undara Basalt|43253|5|Briefly described|map legend|Quaternary||of McBride Basalt Group||||||
18824|Undara Basalt|44246|5|Briefly described|Map Legend||Quaternary|||||||
18824|Undara Basalt|44796|14|Not recorded|p2,3,5|||According to Best 1960, age is Pleistocene.||||||17-JUN-13
18824|Undara Basalt|44926|5|Briefly described|Map Legend||Quaternary|0.19+/- 0.03 Ma, K-Ar||||||
18824|Undara Basalt|45009|14|Not recorded|p96||Pleistocene|Younger than Newer McBride Basalt older than Kinrara Basalt.||||||
18824|Undara Basalt|50198|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||
18824|Undara Basalt|60360|5|Briefly described|Map Legend|Quaternary|Quaternary|Of the McBride Basalt Group. Olivine basalt. Age: 0.19Ma.||||||17-JUN-13
18824|Undara Basalt|68330|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
18824|Undara Basalt|68331|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.||Unit in McBride Basalt Group.|||Vesicular to massive olivine basalt.|
18824|Undara Basalt|68354|5|Briefly described|Map legend.|Quaternary|Quaternary|McBride Basalt Province.|0.19 Ma.||||Olivine basalt.|
18824|Undara Basalt|68405|5|Briefly described|Map Legend|Quaternary|Quaternary|K-Ar dating.|0.19 +/- 0.03 Ma|Of the McBride Basalt Group.|||Vesicular olivine basalt.|
18824|Undara Basalt|68477|5|Briefly described|Map Legend|Pleistocene|Pleistocene|McBride Basalt Province.|ca. 0.19 Ma|Of the McBride Basalt Group.|||Olivine Basalt.|
18824|Undara Basalt|68576|5|Briefly described|Q_11: p19-21|Pleistocene|Pleistocene|Most extensive unit in the McBride Basalt Province, covering 1550 km2. Hosts famous lava tubes. Flows up to 160 km long (world's longest).|190 k.y. (K-Ar).||||Mostly pahoehoe basalt.|
18824|Undara Basalt|73115|6|Mentioned|p: 25, 27-29, 39, 43, 48, 53, 59, 63, 65|Pleistocene|Pleistocene|McBride Basalt Province. Represented by a 160 km long lava flow. No evidence for pyroclastic behaviour. Includes lava tubes. Lava flows appear to bifurcate around basement inliers. Associated with persistent wet areas / springs.|0.19-0.21 Ma|||||
18843|Ungowa beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
18843|Ungowa beach sand|39495|6|Mentioned|p142|||||||||
18843|Ungowa beach sand|62102|5|Briefly described|p367 Tb. 1|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast - forms a coastal strandplain.  Age: 368Ka. See also p371.||||||09-MAY-06
18979|Urannah Igneous Complex|23513|5|Briefly described|Map legend|Permian|Carboniferous|Palaeozoic Intrusive No. 481. I-Type.||||||
18979|Urannah Igneous Complex|30914|6|Mentioned|Map legend|Triassic|Carboniferous|Carboniferous - Cretaceous||||||
18979|Urannah Igneous Complex|31984|6|Mentioned|Map legend|Jurassic|Late Carboniferous|Upper Carboniferous to Lower Cretaceous||||||
18979|Urannah Igneous Complex|32359|5|Briefly described|p735|||||||||
18979|Urannah Igneous Complex|32360|6|Mentioned|p745|||||||||
18979|Urannah Igneous Complex|32553|4|Described|p66|||||||||
18979|Urannah Igneous Complex|32554|4|Described|Table 2|||||||||
18979|Urannah Igneous Complex|32555|6|Mentioned|Map legend|Early Permian|Late Carboniferous|U.Carb.-L.Perm.||||||
18979|Urannah Igneous Complex|32556|4|Described|Table 4|||U.Carb. L.Perm. L.Cret.||||||
18979|Urannah Igneous Complex|35451|6|Mentioned|Table 1|||Summary of rock quarries etc.||||||
18979|Urannah Igneous Complex|35940|6|Mentioned|p637|||||||||
18979|Urannah Igneous Complex|36472|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18979|Urannah Igneous Complex|36528|6|Mentioned|p170|||||||||
18979|Urannah Igneous Complex|36906|6|Mentioned|p25|||||||||
18979|Urannah Igneous Complex|36938|5|Briefly described|p225|||||||||
18979|Urannah Igneous Complex|37458|6|Mentioned|Table 1|||||||||
18979|Urannah Igneous Complex|37675|6|Mentioned|p2|||||||||
18979|Urannah Igneous Complex|38152|6|Mentioned|p354|||||||||
18979|Urannah Igneous Complex|39277|6|Mentioned|p344|||Gold mineralization||||||
18979|Urannah Igneous Complex|39445|5|Briefly described|Table 12|||||||||
18979|Urannah Igneous Complex|41246|6|Mentioned|Map legend|Cretaceous|Carboniferous|||||||
18979|Urannah Igneous Complex|41272|6|Mentioned|M 1of1 E11|||||||||
18979|Urannah Igneous Complex|42547|6|Mentioned|p46|||||||||
18979|Urannah Igneous Complex|43259|4|Described|Appendix 1,p50.|Permian|Carboniferous|||||||
18979|Urannah Igneous Complex|45151|6|Mentioned|p13|||||||||
18979|Urannah Igneous Complex|48921|3|Fully described|p28|||See also Table 2.Upper Carboniferous, Lower Permian&Lower Cretaceous.||||||
18979|Urannah Igneous Complex|48922|6|Mentioned|p20|||||||||
18979|Urannah Igneous Complex|60445|5|Briefly described|p5, p27 Tb. 7|||Part of the Urannah batholith, a composite granitoid pluton. Intrudes the Connors Volcanic Group.||||||
18979|Urannah Igneous Complex|60472|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith. Monzogranite, granodiorite, monzodiorite, granite and gabbro.||||||
18979|Urannah Igneous Complex|60473|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Of the Urannah Batholith.  Gabbro, granodiorite, monzogranite, granite, diorite, aplite, monzodiorite.||||||
18979|Urannah Igneous Complex|60475|5|Briefly described|Map Legend|Early Cretaceous|Late Carboniferous|Heterogeneous assemblage of pink to grey, mainly medium grained granite to diorite; minor gabbro, aplite; rare intrusive breccia.||||||
18979|Urannah Igneous Complex|65706|4|Described|p9 Fig.3; Tb.1 p13,15,p17,18; p23|Early Cretaceous|Late Carboniferous|See also p27 Fig.5, p32 Fig.6, p42 Fig.10, p54, p55-57, p58, p66, p71, p76-77, p103, p116. Hosts gold-bearing mesothermal quartz veins, stockwork and breccias; hosts Ag-Pb-Cu mineralisation. Also appears as Urannah Complex, or Urannah Intrusive Complex, in parts of text.||||Intrudes Connors Volcanic Group, Carmila beds, Calen Coal Measures, Lizzie Creek Volcanic Group; is intruded by Hecate Granite.|Hornblende-biotite granite and granodiorite, hornblende diorite, quartz diorite, biotite granite, hornblende gabbro, hornblende microdiorite with abundant dykes.|
18979|Urannah Igneous Complex|71592|5|Briefly described|Appendix A.|||Connors-Auburn Province, New England Orogen.|284+/-5.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tonalite, dacite dyke.|
19007|Urquhart Shale|22468|5|Briefly described|p 17|Statherian|Statherian|Mount Isa Group||||||
19007|Urquhart Shale|22665|6|Mentioned|P221, Table1||Statherian|Ages of unit are 1652+/-7 Ma and 1654+/-5 Ma||||||
19007|Urquhart Shale|22836|6|Mentioned|Fig.10 p402|||||||||
19007|Urquhart Shale|22961|5|Briefly described|p83||Statherian|||||||
19007|Urquhart Shale|23031|6|Mentioned|27|||Geol province Leichhardt River Subprovince. Parent Mount Isa Group.||||||06-MAY-13
19007|Urquhart Shale|23313|6|Mentioned|319 Fig. 6|||||||||
19007|Urquhart Shale|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group.||||||07-NOV-08
19007|Urquhart Shale|23397|5|Briefly described|p467 Fig.2|||||||||
19007|Urquhart Shale|23398|5|Briefly described|p456|Statherian|Statherian|Mount Isa Group. 1655+/-4Ma. Age from tuff marker bed at Hilton mine. Previous data from tuff marker beds  at Isa mine and Hilton mine provided depositional ages of 1652+/-7 Ma and 1654+/-5 Ma.||||||13-APR-18
19007|Urquhart Shale|23399|4|Described|p485|||Of Mount Isa Group.||||||27-MAY-08
19007|Urquhart Shale|23408|5|Briefly described|p509, p512, p519-20|||Of Mount Isa Group. Rhythmically laminated dolomitic siltstone in the upper section.||||||15-JUN-09
19007|Urquhart Shale|23447|5|Briefly described|p436|||Of Mount Isa Group.||||||27-MAY-08
19007|Urquhart Shale|23466|5|Briefly described|p269|||of Mount Isa Group||||||
19007|Urquhart Shale|23554|6|Mentioned|pB34|||Geological Province: Mt Isa Inlier.||||||
19007|Urquhart Shale|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|1652+/-7 Ma; 1645+/-5 Ma; 1656+/-4 Ma. Of McArthur Group.||||||
19007|Urquhart Shale|23957|6|Mentioned|p1123|Paleoproterozoic|Paleoproterozoic|Age: 1652 +/- 7Ma.||||||07-NOV-08
19007|Urquhart Shale|23961|6|Mentioned|p1191|||Geological Province: Mt Isa Inlier.||||||
19007|Urquhart Shale|23969|6|Mentioned|p1379 Fig.6|||Geological Province: Mount Isa Inlier.||||||02-MAR-05
19007|Urquhart Shale|24168|6|Mentioned|p637|||||||||
19007|Urquhart Shale|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: Mount Isa Group||||||07-NOV-08
19007|Urquhart Shale|24432|4|Described|p560 Tb.1|Statherian|Statherian|Of Mount Isa Group. Age: 1652 Ma. Carbonaceous, pyritic and dolomitic siltstones; tuffaceous horizons. Rhythmically laminated clastic and carbonate facies. Metamorphosed to greenchist facies. Geological Province: Leichardt River Fault Trough.||||||
19007|Urquhart Shale|30192|6|Mentioned|P B209|||||||||
19007|Urquhart Shale|30354|6|Mentioned|p9|||Refers micropalaeontology||||||
19007|Urquhart Shale|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group. Overlies the Native Bee Siltstone; underlies the Spear Siltstone.||||||27-MAY-08
19007|Urquhart Shale|30535|6|Mentioned|p403|||Refers Bennett (1965). See P405 for type section||||||
19007|Urquhart Shale|30722|6|Mentioned|p767|||||||||
19007|Urquhart Shale|30724|6|Mentioned|p74|||||||||
19007|Urquhart Shale|31207|6|Mentioned|p1415|||||||||
19007|Urquhart Shale|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19007|Urquhart Shale|31704|6|Mentioned|p5|||Minor copper in shale association||||||
19007|Urquhart Shale|32041|4|Described|p355|||||||||
19007|Urquhart Shale|32042|4|Described|p38|||||||||
19007|Urquhart Shale|32100|6|Mentioned|p273|||Mt.Isa Gp.||||||
19007|Urquhart Shale|32144|6|Mentioned|p96|||Fossil evidence||||||
19007|Urquhart Shale|32211|6|Mentioned|p12|||Orebodies||||||
19007|Urquhart Shale|32660|5|Briefly described|Table 5|||||||||
19007|Urquhart Shale|32908|6|Mentioned|p5|||Mineralisation||||||
19007|Urquhart Shale|32959|6|Mentioned|p31|||||||||
19007|Urquhart Shale|33111|6|Mentioned|p5|||||||||
19007|Urquhart Shale|33215|6|Mentioned|p1036|||||||||
19007|Urquhart Shale|33900|5|Briefly described|p14|||||||||
19007|Urquhart Shale|34321|6|Mentioned|p5|||See also PP6,7,9 etc||||||
19007|Urquhart Shale|34499|6|Mentioned|Table 1|||||||||
19007|Urquhart Shale|34754|6|Mentioned|p42|||||||||
19007|Urquhart Shale|35074|6|Mentioned|Fig.2|||||||||
19007|Urquhart Shale|35116|6|Mentioned|Table.4|||||||||
19007|Urquhart Shale|35286|6|Mentioned|Fig.17|||||||||
19007|Urquhart Shale|35881|6|Mentioned|p1408|||||||||
19007|Urquhart Shale|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19007|Urquhart Shale|37217|6|Mentioned|p649|||||||||
19007|Urquhart Shale|37568|5|Briefly described|p84|||||||||
19007|Urquhart Shale|37569|6|Mentioned|p93|||||||||
19007|Urquhart Shale|38276|6|Mentioned|p159|||||||||
19007|Urquhart Shale|38345|6|Mentioned|p18|||||||||
19007|Urquhart Shale|38348|6|Mentioned|p11|||||||||
19007|Urquhart Shale|38350|6|Mentioned|p15|||||||||
19007|Urquhart Shale|38618|6|Mentioned|p102|||||||||
19007|Urquhart Shale|39202|6|Mentioned|p242|||||||||
19007|Urquhart Shale|39362|6|Mentioned|p1468|||||||||
19007|Urquhart Shale|39445|5|Briefly described|Table 2|||||||||
19007|Urquhart Shale|39561|6|Mentioned|Fig.8|||||||||
19007|Urquhart Shale|39602|6|Mentioned|p602|||||||||
19007|Urquhart Shale|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
19007|Urquhart Shale|39934|6|Mentioned|p317|||||||||
19007|Urquhart Shale|40394|6|Mentioned|p284|||||||||
19007|Urquhart Shale|40623|5|Briefly described|p95|||||||||
19007|Urquhart Shale|40788|6|Mentioned|p27|||||||||
19007|Urquhart Shale|40847|4|Described|p275|||||||||
19007|Urquhart Shale|41079|6|Mentioned|p296|||||||||
19007|Urquhart Shale|41248|4|Described|p71|||Briefly described P69||||||
19007|Urquhart Shale|41298|6|Mentioned|Map legend|Carpentarian||||||||
19007|Urquhart Shale|41802|5|Briefly described|p530|||||||||
19007|Urquhart Shale|41862|6|Mentioned|p474|||Short Form. Urquhart Shale member used P476||||||
19007|Urquhart Shale|42350|6|Mentioned|Fig.1 P543|||||||||
19007|Urquhart Shale|42570|6|Mentioned|p549|||Short form of name.||||||
19007|Urquhart Shale|42782|6|Mentioned|p458|||of Mount Isa Group||||||
19007|Urquhart Shale|42819|5|Briefly described|p311|||||||||
19007|Urquhart Shale|43610|6|Mentioned|p20|||1652+/-7 Ma||||||
19007|Urquhart Shale|43615|6|Mentioned|p13|||||||||
19007|Urquhart Shale|43760|6|Mentioned|p432|||||||||
19007|Urquhart Shale|44389|14|Not recorded|p33|||No age given. Mineralisation.||||||
19007|Urquhart Shale|44517|2|Defined|p235-237,240-242,map||Paleoproterozoic|Unit of Mount Isa Group. Important. Contains all known economic mineralisation.||||||07-NOV-08
19007|Urquhart Shale|44529|14|Not recorded|p45|||Northern Leases silver-lead-zinc deposit.||||||
19007|Urquhart Shale|44684|14|Not recorded|p1,3,5|||||||||
19007|Urquhart Shale|44685|14|Not recorded|p73,75|||||||||
19007|Urquhart Shale|44764|14|Not recorded|p33-35,37|||||||||
19007|Urquhart Shale|44816|14|Not recorded|p20,22|||||||||
19007|Urquhart Shale|44827|14|Not recorded|p360|||||||||
19007|Urquhart Shale|45072|5|Briefly described|p9|||See also PP10, 35-36 & Table 9. Chem. anal.||||||
19007|Urquhart Shale|45136|5|Briefly described|p50|||||||||
19007|Urquhart Shale|45166|5|Briefly described|p28|||||||||
19007|Urquhart Shale|46801|6|Mentioned|Table 1|||See also Fig. 14. Stratigraphy||||||
19007|Urquhart Shale|47011|6|Mentioned|p332|||||||||
19007|Urquhart Shale|50332|5|Briefly described|p21, p95|Proterozoic|Proterozoic|Of the Mount Isa Group. Overlain by Spear Siltstone. Geological Province: Western Fold Belt Province. Consists of ferruginous pyritic shale and pyritic siltstone with tuff marker beds.||||||07-FEB-11
19007|Urquhart Shale|50624|3|Fully described|p233||Statherian|U-Pb ages:1652+-7 Ma; 1655 +-4 Ma. Fine grained with carbonaceous and muddy layers. Five subdivisions described. Dip: 30-80 degrees W. Parent: Mount Isa Group. Overlies Native Bee Siltstone, overlain by Spear Siltstone.||||||
19007|Urquhart Shale|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Overlain by Spear Siltstone, underlain by Native Bee Siltstone. Geological Province: Western Fold Belt.||||||
19007|Urquhart Shale|61204|3|Fully described|p538, p539|Statherian|Paleoproterozoic|Geol Prov: Mount Isa Inlier. Of Mount Isa Group. Underlain by Haslingden Group. Age: 1652+/-7 Ma and 1655+/-4 Ma (Page and Sweet, 1998; Page et al., 2000).Maximum thickness: 6 Km. Carbonaceous, dolomitic siltstones, mudstones and shales.||||||31-MAY-07
19007|Urquhart Shale|61736|5|Briefly described|p673|Paleoproterozoic|Paleoproterozoic|Age: 1652+/-7Ma.||||||
19007|Urquhart Shale|61923|5|Briefly described|p30 Fig.3|Paleoproterozoic|Paleoproterozoic|Contains tuff layers with age of 1652+/-7 Ma. Overlies Native Bee Siltstone.||||||07-NOV-08
19007|Urquhart Shale|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1655+/-4Ma. Geological Province: Isa Superbasin, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
19007|Urquhart Shale|62084|4|Described|p936 Fig.5, p950-953|||Isa Superbasin. Mount Isa. Hosts Mount Isa, Hilton and George Fisher deposits (each containing >100 Mt of high-grade stratiform Zn-Pb-Ag; occurs within upper 650 m). Thickness: 1000 m. Age : ~1653 Ma (Page and Sweet 1988, Fig.6).|1655+/-4 Ma U-Pb SHRIMP (after Page et al. 2000)|Mount Isa Group|||Distinctive assemblage of mudstone, pyritic siltstone, and tuffaceous lithofacies. Variably dolomitic organic siltstones and shales.|
19007|Urquhart Shale|62473|5|Briefly described|p75|Paleoproterozoic|Paleoproterozoic|Ages: 1654+/-5Ma, 1656+/-4Ma and 1652+/-7Ma (tuff). This is the mineralised host of the Mount Isa and Hilton orebodies.||||||
19007|Urquhart Shale|62535|5|Briefly described|p672-674|Statherian|Statherian|Leichhardt River Fault Trough. Lithology not specified on p672.|1655 +/- 4 Ma.|Mount Isa Group.|||Includes fine, silty dolomite.|
19007|Urquhart Shale|62873|5|Briefly described|p692|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group. Interbedded siltstones and shales; hosts the Mount Isa copper deposit and lead-zinc deposits at Mount Isa, Hilton and George Fisher. Contains tuff marker beds. Age: 1652+/-7Ma and 1655+/-4Ma (SHRIMP zircon ages - Page and Sweet, 1998).||||||07-NOV-08
19007|Urquhart Shale|63023|6|Mentioned|p1037|Paleoproterozoic|Paleoproterozoic|Age: ca 1660-1655Ma. Of the Gun Supersequence.||||||07-NOV-08
19007|Urquhart Shale|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Isa Superbasin.||||||30-SEP-08
19007|Urquhart Shale|63111|5|Briefly described|p1163 Fig. 3|Statherian|Statherian|Of Gun Supersequence. Ages: 1668 - 1653Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, dolomudstones, laminated carbonates.||||||06-MAY-13
19007|Urquhart Shale|63113|6|Mentioned|p1225 Fig.13. |||Isa Superbasin. Part of Gun supersequence.||||||
19007|Urquhart Shale|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin. Appears only as Urquhart.||||||
19007|Urquhart Shale|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
19007|Urquhart Shale|63116|6|Mentioned|p1297 Fig.2, |||Isa superbasin.||||||
19007|Urquhart Shale|63866|5|Briefly described|p59|Statherian|Statherian|Isa Superbasin.|1652 +/- 7 Ma (Page et al., 2000)|Gun Supersequence||||
19007|Urquhart Shale|63884|5|Briefly described|p14|||Equivalent to Paradise Creek Formation.||||||
19007|Urquhart Shale|64250|6|Mentioned|p11 fig 3, p20|||At Mount Isa. Hosts the Pb-Zn-Ag-Cu mineralisation.|1655 +/- 4 Ma|Unit in Mount Isa Group.||||
19007|Urquhart Shale|64367|5|Briefly described|p555  Fig. 1c, p561 Tb. 2|Paleoproterozoic|Paleoproterozoic|Upper unit in Mount Isa Group. Ages: 1655+/-4Ma, 1652+/-7Ma. Carbonaceous dolomitic interbedded siltstones and shales, and hosts the Mount Isa Cu deposit in a discordant syntectonic breccia system; also contains interbedded tuffs, potassic-altered.||||||07-FEB-11
19007|Urquhart Shale|65228|5|Briefly described|Fig.04.|Statherian|Statherian|Mount Isa area.|1655 +/- 4 Ma and 1652 +/- 7 Ma.|||||
19007|Urquhart Shale|65396|5|Briefly described|p82, p175, p188, p195, p241|Statherian|Statherian|Isa Superbasin. Cover Sequence 3. Leichhardt River Fault Trough. Host to Pb-Zn-Ag-Cu mineralization at Mount Isa. Detrital zircon sources listed.|1655 +/- 4 Ma|Mount Isa Group||Overlies Native Bee Siltstone; overlain by Spear-Kennedy Siltstone.||04-APR-17
19007|Urquhart Shale|66824|6|Mentioned|p148|||Previously dated at 1670 +21/-17 Ma (Page, 1981). New SHRIMP zircon age is 1653 +/- 7 Ma (R.W.Page, unpubl. data).||Mount Isa Group.|||Contains tuff horizons (whence the age determination).|
19007|Urquhart Shale|66843|5|Briefly described|p35|||Contains "cross fracture tuff marker beds" compared with carbonate-filled "cross fractures" in the Amos Formation, McArthur Group.||Mount Isa Group.||||
19007|Urquhart Shale|66844|5|Briefly described|p245|Statherian|Statherian|Mount Isa region. SHRIMP zircon ages of 1652+\-7, 1654+\-5 and 1656+\-4 Ma. See also Urquhart Formation p244.||Within Gun Supersequence. Of lower McNamara Group.||||
19007|Urquhart Shale|67026|4|Described|pp336-340, p342 Fig.9, p344.|Statherian|Statherian|Hosts the Mount Isa and George Fisher Zn-Pb-Ag(-Cu) mineralisations. George Fisher mineralisation is hosted by laminated pyritic siltstone. The Mount Isa ores are grossly strata-bound and stratiform, with common pyrrhotite, and include Cu. Magnetisation is discussed in detail and dated at 1505 +/- 10 Ma, the waning of the Isan orogeny.|c.1655 +/- 4 Ma (Page et al. 2000).|Unit in Mount Isa Group.|||Interbedded siltstones and shales.|24-APR-12
19007|Urquhart Shale|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot; p26, p34. Leichhardt River Domain, Isa Superbasin.|1652 +/- 7 Ma.|Mount Isa Group.|||Grey pyritic siltstone, tuff marker beds.|
19007|Urquhart Shale|67499|5|Briefly described|p938, 939, 940, 941, 944-946, 948, 949|Statherian|Statherian|Age has been estimated using SHRIMP U-Pb dating of zircons from tuffaceous meta-sediments, but note pervasive hydrothermal alteration. Hosts base metal deposits.|1655 +/- 4 Ma|Of Mount Isa Group?|||Significant base metal host and is characterised by enrichment in carbon and regular interlayering of mechanically contrasting meta-shale and meta-siltstone.|
19007|Urquhart Shale|68020|6|Mentioned|p126|||Contains Mount Isa Cu mineralization.||Mount Isa Group||||
19007|Urquhart Shale|68542|6|Mentioned|p6|||||||Overlies Native Bee Siltstone, overlain by Spear Siltstone||
19007|Urquhart Shale|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier. Hosts the George Fisher Hilton Mount Isa Zn-Pb-Ag deposit.||Mount Isa Group.||Overlies Native Bee Siltstone. Is overlain by Spear Siltstone.||
19007|Urquhart Shale|68732|5|Briefly described|p160, p162-163, p165 Fig.3, p169|Statherian|Statherian|Of the Gun Supersequence. Sedimentary depositional age.|1652 +/- 7 Ma  sedimentary depositional age|Of the Mount Isa Group.|||Siliciclastic sediments: monotonous intervals of massive to finely-laminated siltstone and shale, up to several hundred of metres thick.|01-DEC-17
19007|Urquhart Shale|69542|6|Mentioned|p132, p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Hosts the giant Mt Isa stratiform and stratabound Pb-Zn-Ag and Cu-Au deposits. Western Fold Belt.||Mount Isa Group||||09-FEB-18
19007|Urquhart Shale|69591|4|Described|p43, p45|||Isa Superbasin. Part of Gun Supersequence. Deposited below storm base. Hosts the giant Mount Isa Pb, Zn and Cu orebodies.|1652 +/- 7 Ma (Page and Sweet, 1998).|Mount Isa Group.||Equated with Esperanza Formation.|Grey pyritic siltstone, tuff marker beds.|
19007|Urquhart Shale|70282|5|Briefly described|p544, p546, p558|||Hosts the globally significant Mount Isa base metal (Cu-Zn-Pb-Ag) deposit. Beds have an average thickness of 11.6mm.||Mount Isa Group||Overlain by Kennedy, Spear Siltstones; overlies Native Bee Siltstone, Eastern Creek Volcanics|Interbedded dolomitic shales, siltstones and mudstones.|13-FEB-18
19007|Urquhart Shale|70283|5|Briefly described|p25, p26|Statherian|Statherian|Contains Pb-Zn-Ag and Cu ore deposits. Age from zircons in tuffaceous beds.|1653 +/- 7 Ma (Connors and Page, 1995).|Mount Isa Group|||Pyritic and dolomitic siltstones, shales and tuffaceous beds.|14-FEB-18
19007|Urquhart Shale|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1654+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuffaceous shale, ash tuff.|
19007|Urquhart Shale|71960|6|Mentioned|p80|||Shows post-main phase folds at Mount Isa Mine.||||||
19007|Urquhart Shale|72297|6|Mentioned|p708|||Hosts the copper mineralisation at Mount Isa.||||||
19007|Urquhart Shale|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province. Ages given as U-Pb zircon sedimentary depositional ages.|1654 +/-5 Ma, 1652 +/-7 Ma|Mount Isa Group||Overlies Native Bee Siltstone and underlies Spear-Kennedy Siltstone.||
19007|Urquhart Shale|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province.  U-Pb zircon sedimentary depositional ages given.|1654 +/- 5 Ma,1652 +/- 7 Ma|Mount Isa Group||Overlies Native Bee Siltstone and underlies Spear-Kennedy Siltstone.||
19007|Urquhart Shale|73042|6|Mentioned|p4||Statherian|Mount Isa Province, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1652 +/- 7 Ma, 1654 +/- 5 Ma (see Fig.1.2)|Mt Isa Group||Underlain by Native Bee Siltstone. Overlain by Spear-Kennedy Siltstone.||
19007|Urquhart Shale|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Leichhardt River Domain.|1652+/-7 Ma, 1655+/-4 Ma||||Carbonates.|
19024|V-Creek Limestone|23031|5|Briefly described|19|||||||||
19024|V-Creek Limestone|23393|5|Briefly described|p23 Fig. 6|Cambrian|Cambrian|Geological Province: Georgina Basin.||||||
19024|V-Creek Limestone|23408|6|Mentioned|p527|||Includes two-toned deeper-water ramp carbonates.||||||15-JUN-09
19024|V-Creek Limestone|30242|6|Mentioned|Fig.2|||||||||
19024|V-Creek Limestone|30479|6|Mentioned|Fig.6|||See also Fig.7. Stratigraphic relationships||||||
19024|V-Creek Limestone|30914|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
19024|V-Creek Limestone|31396|6|Mentioned|Fig.3|||||||||
19024|V-Creek Limestone|33111|4|Described|p44|||||||||
19024|V-Creek Limestone|33482|6|Mentioned|Fig.5|||Middle Cambrian||||||
19024|V-Creek Limestone|34395|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
19024|V-Creek Limestone|35054|6|Mentioned|Table 23|||||||||
19024|V-Creek Limestone|35121|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
19024|V-Creek Limestone|35139|4|Described|Table.2|||||||||
19024|V-Creek Limestone|35553|6|Mentioned|p36|||See also Appendix 2, description of Agnostid localities.||||||
19024|V-Creek Limestone|35556|6|Mentioned|Plate 35|||||||||
19024|V-Creek Limestone|37275|6|Mentioned|p287|||||||||
19024|V-Creek Limestone|37572|4|Described|p158|||||||||
19024|V-Creek Limestone|38444|6|Mentioned|p106|||||||||
19024|V-Creek Limestone|38445|6|Mentioned|p105|||||||||
19024|V-Creek Limestone|38446|6|Mentioned|Table 23|||||||||
19024|V-Creek Limestone|39445|5|Briefly described|Table 4|||See also p62.||||||13-DEC-06
19024|V-Creek Limestone|39690|6|Mentioned|p88|||||||||
19024|V-Creek Limestone|40038|6|Mentioned|p248|||||||||
19024|V-Creek Limestone|40686|5|Briefly described|p407|||||||||
19024|V-Creek Limestone|40856|6|Mentioned|Fig.23.6|||||||||
19024|V-Creek Limestone|41298|6|Mentioned|Map legend|Middle Cambrian||||||||
19024|V-Creek Limestone|41388|6|Mentioned|Fig.2|||||||||
19024|V-Creek Limestone|44091|14|Not recorded|p16,Tb.1,18||Middle Cambrian|||||||
19024|V-Creek Limestone|44205|14|Not recorded|p50-1,61,67,140,155,|||p167,168||||||
19024|V-Creek Limestone|44210|2|Defined|map,Tb.2,p13,14|||||||||
19024|V-Creek Limestone|44211|14|Not recorded|p101,103,107|||Known only in Undilla Basin. See also Lexicon.||||||
19024|V-Creek Limestone|44213|14|Not recorded|Map Legend||Middle Cambrian|||||||
19024|V-Creek Limestone|44275|14|Not recorded|Map Legend|||||||||
19024|V-Creek Limestone|44920|14|Not recorded|Map Legend,||Middle Cambrian|||||||
19024|V-Creek Limestone|45012|14|Not recorded|p338|||||||||
19024|V-Creek Limestone|45054|6|Mentioned|p6|||Fossil locality||||||
19024|V-Creek Limestone|45079|5|Briefly described|p34|||Cambrian age||||||
19024|V-Creek Limestone|45119|6|Mentioned|p3|||||||||
19024|V-Creek Limestone|48633|14|Not recorded|p99|||Ref. to Opik 1961.||||||
19024|V-Creek Limestone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: eastern Georgina Basin.||||||
19024|V-Creek Limestone|63450|5|Briefly described|p82|Middle Cambrian|Middle Cambrian|Geological Province: Undilla Sub-basin.||||||07-FEB-11
19024|V-Creek Limestone|64068|6|Mentioned|p62, 193|||Northeastern Georgina Basin. Correlated with  Arthur Creek Formation, Blazan Shale, Roaring Siltstone.. [See also misspelling: V Creek Limestone, p63 etc] Hosts limestone suitable for metallurgical lime, quicklime and cement manufacture, but operations are not viable due to transport difficulties and excessive energy requirements.||||Conformably overlies Inca Formation.||05-APR-12
19024|V-Creek Limestone|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map; p83|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||Narpa Group.||Overlies Currant Bush Limestone. Is overlain by Mail Change Limestone.|Limestone, bituminous limestone, sandy limestone, calcilutite, minor arenite, chert nodules.|
19024|V-Creek Limestone|69443|5|Briefly described|p28:16, 24-25|Middle Cambrian|Middle Cambrian|Georgina Basin.||Narpa Group.||Correlated with Ranken Limestone and Camooweal Dolostone.||12-JUL-16
19024|V-Creek Limestone|69573|6|Mentioned|p659|||Contains Drumian Stage [Cambrian] fossil sites.||||||
19024|V-Creek Limestone|69591|5|Briefly described|p87|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Mostly appears as V Creek Limestone (p88, p90, p96-97, p98 Fig.2.91). Coeval with Camooweal Dolostone.||Narpa Group.||Overlies Currant Bush Limestone. Is overlain by Mail Change Limestone.||
19024|V-Creek Limestone|72321|6|Mentioned|Fig 2|Drumian|Drumian|Undilla Sub-basin, Georgina Basin. Australian Stages: Floran to Undillan.||of Narpa Group.||||
19024|V-Creek Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Eastern Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
19024|V-Creek Limestone|72967|6|Mentioned|p5|||Georgina Basin.||Napa Group||||
19024|V-Creek Limestone|73418|5|Briefly described|p4 Fig.3|Miaolingian|Miaolingian|Georgina Basin, Undilla Sub-basin.||Narpa Group||Overlies Currant Bush Limestone, underlies Mail Change Limestone|Limestone.|
19045|Van Dyke Litharenite|23423|4|Described|p303 Table 7.2||Late Ordovician|Faulted against and unconformable on the Mulgrave Formation. Age is unknown but similarities with the Mount Creek Conglomerate suggest they are equivalent. Also see p232.||||||
19045|Van Dyke Litharenite|23430|4|Described|p471-473|||Hodgkinson Province.||||||
19045|Van Dyke Litharenite|23431|6|Mentioned|p539|||||||||
19045|Van Dyke Litharenite|23713|5|Briefly described|p35||Late Ordovician|Hodgkinson Province.||||||
19045|Van Dyke Litharenite|41824|6|Mentioned|p201|||||||||
19045|Van Dyke Litharenite|42500|5|Briefly described|p11|||||||||
19045|Van Dyke Litharenite|42620|3|Fully described|p60|||||||||
19045|Van Dyke Litharenite|43083|3|Fully described|p29, p31 Tb. 2||Late Ordovician|Geological province: Hodgkinson Province. Mainly lithic and felspathic arenite.||||||17-JUN-09
19045|Van Dyke Litharenite|43285|5|Briefly described|Map Legend||Late Ordovician|||||||
19045|Van Dyke Litharenite|43625|4|Described|p19,20|||Age: ?Late Ordovician||||||
19045|Van Dyke Litharenite|60357|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Geological Province: Hodgkinson Province. Arenite, shale, siltstone.||||||
19045|Van Dyke Litharenite|60425|3|Fully described|p13, p18 Tb. 1, p21|Late Ordovician|Late Ordovician|Faulted against Mulgrave Fm. Age: probably Late Ord.- no diagnostic fossils found. Geol.prov: Hodgkinson Province. Rhythmically interbedded thin to med.bedded arenite + mudstone; minor haematitic mudstone and chert (jasper) and rare conglomeratic arkose||||||07-FEB-11
19045|Van Dyke Litharenite|62371|5|Briefly described|p472 Fig.3|Ordovician|Ordovician|Mixed shallow marine sediments.||||||
19045|Van Dyke Litharenite|63140|5|Briefly described|p570, p572 Fig.3, p582, p583 Fig.13.|Late Ordovician|Late Ordovician|Product of arc-magmatism during major eustatic episode.||||Overlies Mulgrave Formation unconformably.||
19045|Van Dyke Litharenite|63154|5|Briefly described|p281 Fig. 3|Late Ordovician|Late Ordovician|Geological province: Hodgkinson Province. Mixed shallow marine sediments.||||||11-APR-07
19045|Van Dyke Litharenite|67848|5|Briefly described|p16.|||Western margin of Hodgkinson Province. Undated; possibly Ordovician. Comparable rock assemblage to the arc assemblage and Wairuna Formation of Broken River Province.|||||Includes volcaniclastics.|
19045|Van Dyke Litharenite|68553|6|Mentioned|Map legend; schematic diagram.|Ordovician|Ordovician|Mount Windsor Subprovince. This unit, as well as Mountain Creek and Quadroy Conglomerates, and Mulgrave Formation, are all mapped under the symbol, Om.||||||
19045|Van Dyke Litharenite|69030|6|Mentioned|p6|Silurian|Ordovician|Chillagoe Subprovince, Hodgkinson Province.||||||
19045|Van Dyke Litharenite|69079|6|Mentioned|p3-4|||Hodgkinson Province.||||||
19045|Van Dyke Litharenite|69592|5|Briefly described|p230, p231 Fig.4.4, p232, p297,p301,p304|Ordovician|Ordovician|Chillagoe Subprovince, Hodgkinson Province. Crops out in two discontinuous, N-trending, topographically recessive belts up to 20km x 1km, alternating with ridges of Mulgrave Formation (both units referred to as Thomson Orogen strata). Deposition by density currents including turbidity flows. Provisional age is based on similarities with nearby units.||||Is structurally intercalated with Mulgrave Formation.|Rhythmically interbedded, thin- to medium-bedded sandstone and mudstone, with minor thick-bedded, grey, hematitic mudstone, hematitic chert and rare pebbly feldspathic sandstone; one silicic volcanic interbed.|
19045|Van Dyke Litharenite|70207|6|Mentioned|p74|||Included in a group of units collectively aged as Ordovician-Silurian & Carboniferous?.||||||
19045|Van Dyke Litharenite|70345|6|Mentioned|p3|Carboniferous|Late Ordovician|||||||
19045|Van Dyke Litharenite|70673|6|Mentioned|p7|||Age (range) given as "Late Ordovician & Carboniferous?[sic]".||||||
19045|Van Dyke Litharenite|71031|6|Mentioned|p70, p72|||Included in the Thomson Orogen by Henderson and Donchak (2013).||||||
19045|Van Dyke Litharenite|72983|6|Mentioned|p15|Carboniferous?|Ordovician|Thomson Orogen.||||||
19058|Vanneck Formation|23422|5|Briefly described|p180, p206 Table 6.3|Late Devonian|Late Devonian|Of Dotswood Group.||||||
19058|Vanneck Formation|23424|6|Mentioned|p346||Frasnian|Overlain by Julia Formation. Burdekin Basin Province.||||||13-NOV-07
19058|Vanneck Formation|23430|5|Briefly described|Plate 14.11 + p505||Devonian|Of Dotswood Group. Overlain by Stud Formation. Burdekin Basin Province.||||||13-NOV-07
19058|Vanneck Formation|23431|5|Briefly described|p538|||Of Dotswood Group.||||||08-OCT-08
19058|Vanneck Formation|23509|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Dotswood Group.||||||08-OCT-08
19058|Vanneck Formation|23522|5|Briefly described|p250 Fig 6|Famennian|Givetian|||||||
19058|Vanneck Formation|23893|5|Briefly described|p16|Late Devonian|Late Devonian|Of Dotswood Group.  Geological Province: Burdekin Basin.||||||
19058|Vanneck Formation|24577|4|Described|p752 Fig. 1|Frasnian|Eifelian|Of the Dotswood Group. Overlain by the Stud Formation. Overlies the Fanning River Group. Formation is Fm in text. Geological Province: Burdekin Basin, Lachlan Fold Belt.||||||08-OCT-08
19058|Vanneck Formation|24613|2|Defined|p9 Fig. 4, p37-39|Frasnian|Frasnian|Of Dotswood Gp. Dis/un-conformably on Cultivation Gully Formation; conformable below Stud Fm.Max. thickness: 360m. Geol.province: Burdekin Basin. Sandstone, mudstone, siltstone, minor conglomerate. Comprises 4 lithological facies - details included||||||07-FEB-11
19058|Vanneck Formation|24614|5|Briefly described|p191 Fig. 1|Frasnian|Frasnian|Of Dotswood Gp. Formerly basal unit of Dotswood Gp; redefined by Lang et al (1990a). Green to red volcaniclastic Sst, + generally minor quartzose + polymictic conglom, tuffs + algal Lst + red mudstones. Geol Prov: Burdekin Basin. See also p193 Fig. 2.||||||07-FEB-11
19058|Vanneck Formation|31285|4|Described|p82|||Frasnian. Unit of Dotswood Gp.||||||
19058|Vanneck Formation|37573|4|Described|p210|||See also Figs.7 and 8 and p208.||||||13-NOV-07
19058|Vanneck Formation|38374|6|Mentioned|p600|||||||||
19058|Vanneck Formation|39445|5|Briefly described|Table 6|||||||||
19058|Vanneck Formation|39686|4|Described|p78|||||||||
19058|Vanneck Formation|39732|6|Mentioned|p29|||||||||
19058|Vanneck Formation|42689|5|Briefly described|map legend|Late Devonian||||||||
19058|Vanneck Formation|42690|5|Briefly described|map legend|Carboniferous|Late Devonian|||||||
19058|Vanneck Formation|42933|5|Briefly described|p257|||||||||
19058|Vanneck Formation|43095|5|Briefly described|Plate 2|||Of Dotswood Group.||||||08-OCT-08
19058|Vanneck Formation|43933|5|Briefly described|Map Legend||Late Devonian|Of Dotswood Group.||||||
19058|Vanneck Formation|62522|2|Defined|p22|Frasnian|Givetian|Of Dotswood Gp. Includes: Clayhole Tuff Mbr.Parts overlie Cultivation Gully and Burdekin Fms, Fanning River Gp; transitional below Stud Fm. Thick: ~360m. Sandstone, mudstone, siltstone + minor conglom. Four detailed lithologies are given (Lang et al 1990)||||||13-NOV-07
19058|Vanneck Formation|65214|6|Mentioned|p279, p280, p283|Devonian|Devonian|QLD, Burdekin. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19058|Vanneck Formation|67402|4|Described|p239, p247, p248|Frasnian|Frasnian|Burdekin Basin. Unsuitable reservoir for the storage of carbon dioxide. Deposited under coastal plain, alluvial fan or floodplain/lacustrine conditions.||||Overlain by the Stud Formation.|Sandstone, mudstone and siltstone with minor conglomerate, tuff and limestone.|
19058|Vanneck Formation|68350|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Burdekin Formation. Is overlain conformably by Stud Formation.|Green to red, volcaniclastic sandstone, mudstone, siltstone, minor conglomerate, green tuff, algal limestone (fish and plant fossils).|
19058|Vanneck Formation|68351|5|Briefly described|Map legend.|Late Devonian|Late Devonian|Burdekin Basin.||Unit in Dotswood Group.||Conformably overlies Burdekin Formation. Is overlain conformably by Stud Formation.|Green to red, volcaniclastic sandstone, mudstone, siltstone, minor conglomerate, green tuff, algal limestone (fish and plant fossils).|
19058|Vanneck Formation|68419|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin. Includes an informal unnamed subunit.||Of the Dotswood Group.||Conformably overlain by the Stud Formation. Conformably underlain by the Burdekin Formation, Fanning River Group.|Green to red, volcaniclastic sandstone, mudstone, siltstone, minor conglomerate, green tuff, algal limestone (fish and plant fossils); quartzose and polymictic conglomerate and very coarse-grained sandstone and minor red mudstone.|
19058|Vanneck Formation|68420|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Burdekin Basin. Includes an informal unnamed subunit.||Of the Dotswood Group.||Conformably overlain by the Stud Formation. Conformably underlain by the Burdekin Formation, Fanning River Group.|Green to red, volcaniclastic sandstone, mudstone, siltstone, minor conglomerate, green tuff, algal limestone (fish and plant fossils); quartzose and polymictic conglomerate and very coarse-grained sandstone and minor red mudstone.|
19058|Vanneck Formation|68731|5|Briefly described|p177 Fig 3.91, p185 Tb 3.4, p186|Late Devonian|Late Devonian|Burdekin Basin. < 350 m thick. Sandy coastal plain; contemporary volcanism; ephemeral lake development. Depositional environment discussed.||Of the Dotswood Group.|Includes the Clayhole Tuff Member.||Comprises fine to very coarse volcaniclastic sandstone, pebbly sandstone and siltstone (commonly red). Basal pebbly to cobbly polymict or volcaniclastic conglomerate. Rare ignimbrite and lacustrine limestone and chert beds.|27-AUG-14
19176|Wade beds|23032|4|Described|p46|Early Permian|Late Carboniferous|Originally included in Clarke River Group.||||||
19176|Wade beds|23422|6|Mentioned|p183|||Geological Province: Clarke River Basin.||||||
19176|Wade beds|23424|4|Described|Table 8.1 Fig 8.4 p339.|Early Permian|Late Carboniferous|Age determined with plant macrofossils and palynomorphs. Unconformably overlies Carboniferous Clarke River Group and faulted against the Silurian Graveyard Creek Group. Underlying Unit Clarke River Group (unconformably). Maximum thickness ~84 m+||||||
19176|Wade beds|23430|5|Briefly described|p504 Table 14.5|||Also see p520. Underlying Unit Clarke River Group. Clarke River Basin Province. Maximum thickness 84 m.||||||
19176|Wade beds|42692|5|Briefly described|map legend|Permian|Late Carboniferous|Not a variation on Wade Sandstone, WA or Wade Creek Sandstone, NT & WA.||||||
19176|Wade beds|42752|6|Mentioned|p48|||||||||
19176|Wade beds|42933|4|Described|p214|||Intended as informal use.||||||
19176|Wade beds|43095|6|Mentioned|p75|||||||||
19176|Wade beds|43286|5|Briefly described|Map Legend|Permian|Late Carboniferous|||||||
19176|Wade beds|68336|5|Briefly described|Map legend.|Early Permian?|Late Carboniferous|Clarke River Basin.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68339|5|Briefly described|Map legend.|Early Permian?|Late Carboniferous|Galilee Basin outlier.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68340|5|Briefly described|Map legend.|Early Permian?|Late Carboniferous|Galilee Basin outlier.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68341|5|Briefly described|Map legend.|Early Permian?|Late Carboniferous|Clarke River Basin.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68478|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Galilee Basin Outlier. Fluvial and lacustrine sedimentary rocks.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68479|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Galilee Basin Outlier. Fluvial and lacustrine sedimentary rocks.|||||Sublabile to labile sandstone, siltstone, carbonaceous mudstone and minor conglomerate.|
19176|Wade beds|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Broken River Province. This unit, as well as Balfes Creek and Ellenvale beds; Insolvency Gully and Marshs Creek Formations; and Silver Valley Conglomerate, are all mapped under the symbol, CPs.||||||
19176|Wade beds|68576|6|Mentioned|Q_11: p38|||Camel Creek Subprovince.||||||
19176|Wade beds|69592|5|Briefly described|p258, p274 Fig.4.65, p276, p279|Permian|Pennsylvanian|Draper, Scott and Withnall (1993). Wade Basin. <300m thick. Age range from flora and palynomorphs.||Sybil Group.||Unconformably overlies Clarke River Group. Correlative of the Sybil Group.|Interbedded sandstone, mudstone and some conglomerate and minor coaly beds and carbonaceous plant-bearing horizons.|
19210|Wairuna Formation|23032|4|Described|p17,34||Ordovician|||||||
19210|Wairuna Formation|23291|6|Mentioned|p30|||Geological Province: Georgetown Region.||||||08-JUL-15
19210|Wairuna Formation|23424|4|Described|Table 8.1 Fig 8.2/8.3 p331.||Ordovician|Age: Unfossiliferous but probably Ordovician because of similarities to Judea Fm. Faulted against Halls Reward Metamorphics along Burdekin Fault. Intruded by tectonically emplaced serpentinite, & by Princess Hills Granite.  Camel Creek Subprovince.||||||
19210|Wairuna Formation|23430|5|Briefly described|p476|||Age uncertain, inferred to be Ordovician. Broken River Province.||||||
19210|Wairuna Formation|23431|5|Briefly described|p541|||||||||
19210|Wairuna Formation|23494|4|Described|p9, p23 Tb. 1|Wenlock|Llandovery|Unconformably overlain by Graveyard Creek Formation.  Intruded by Herbert River Granite.  Max. thickness: 5000ft?||||||
19210|Wairuna Formation|23498|5|Briefly described|p23 table 1||Early Silurian|Unconformably overlain by Graveyard Creek Formation||||||
19210|Wairuna Formation|23616|5|Briefly described|Table 1C p15|||May be equivalent to Mulgrave Formation. Broken River Province.||||||
19210|Wairuna Formation|23619|4|Described|p34 Table 1|||Faulted against Halls Reward Metamorphics. Intruded by Carboniferous Princess Hills granite. Broken River Province.||||||
19210|Wairuna Formation|23713|6|Mentioned|p13|||||||||
19210|Wairuna Formation|23893|6|Mentioned|p14|||||||||
19210|Wairuna Formation|24074|5|Briefly described|p389 Table 1|Silurian|Late Ordovician|||||||
19210|Wairuna Formation|24485|6|Mentioned|p27|||||||||
19210|Wairuna Formation|24577|4|Described|p752 Fig. 1, p762|Ordovician|Ordovician|Overlain by the Everetts Creek Volcanics and the Carriers Well Formation"". Overlies the Judea Formation. Formation is Fm in text. Geological Province: Broken River Region, Lachlan Fold Belt. Formerly referred to as Carriers Well Formation.||||||
19210|Wairuna Formation|29445|5|Briefly described|p77|||||||||
19210|Wairuna Formation|30334|6|Mentioned|p120|||||||||
19210|Wairuna Formation|30914|6|Mentioned|Map legend|Devonian|Silurian|Ordovician - Devonian||||||
19210|Wairuna Formation|31832|6|Mentioned|Table 6|||||||||
19210|Wairuna Formation|31999|6|Mentioned|Table 11|||Fig. 3||||||
19210|Wairuna Formation|32553|4|Described|p52|||||||||
19210|Wairuna Formation|33434|6|Mentioned|Fig.2|||||||||
19210|Wairuna Formation|34252|6|Mentioned|Ps.6|||Fossils||||||
19210|Wairuna Formation|34346|6|Mentioned|p1|||Lower Silurian. See also p11,12.||||||19-APR-18
19210|Wairuna Formation|35008|6|Mentioned|p179|||||||||
19210|Wairuna Formation|35197|6|Mentioned|p352|||||||||
19210|Wairuna Formation|35554|6|Mentioned|p5|||||||||
19210|Wairuna Formation|36472|6|Mentioned|Map legend|Early Silurian|Ordovician|Early Silurian to Ordovician||||||
19210|Wairuna Formation|37575|4|Described|p181|||See also Fig.3||||||
19210|Wairuna Formation|37727|4|Described|p92|||See also p21 and p31.||||||19-APR-18
19210|Wairuna Formation|37768|5|Briefly described|p41|||See also p40.||||||19-APR-18
19210|Wairuna Formation|37769|6|Mentioned|Fig.11|||||||||
19210|Wairuna Formation|37770|6|Mentioned|Fig.12|||||||||
19210|Wairuna Formation|39027|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
19210|Wairuna Formation|39445|5|Briefly described|Table 4|||See also p64, p74, Table 5 & Fig.6||||||19-APR-18
19210|Wairuna Formation|39686|6|Mentioned|Fig.1|||||||||
19210|Wairuna Formation|39689|6|Mentioned|p52|||See also Fig.3 and p62.||||||19-APR-18
19210|Wairuna Formation|40623|5|Briefly described|p92|||||||||
19210|Wairuna Formation|40787|6|Mentioned|p324|||See also Fig.2||||||
19210|Wairuna Formation|40943|6|Mentioned|p50|||||||||
19210|Wairuna Formation|41260|3|Fully described|p10|||Described p139. See also p23||||||19-APR-18
19210|Wairuna Formation|41675|6|Mentioned|p15|||||||||
19210|Wairuna Formation|41679|6|Mentioned|Fig.1|||||||||
19210|Wairuna Formation|41719|6|Mentioned|Fig.1|||||||||
19210|Wairuna Formation|41739|6|Mentioned|Fig.1|||See also Fig.2||||||
19210|Wairuna Formation|42031|5|Briefly described|Fig.4 p761|||||||||19-APR-18
19210|Wairuna Formation|42279|6|Mentioned|Fig.2 P18|||||||||
19210|Wairuna Formation|42692|5|Briefly described|map legend|Ordovician||||||||
19210|Wairuna Formation|42693|5|Briefly described|map legend|Ordovician||||||||
19210|Wairuna Formation|42747|6|Mentioned|p36|||||||||
19210|Wairuna Formation|42752|5|Briefly described|p45|||see also Fig.2 p46, Fig.3 p47.||||||19-APR-18
19210|Wairuna Formation|42933|3|Fully described|p19|||||||||
19210|Wairuna Formation|43060|5|Briefly described|p39|||||||||
19210|Wairuna Formation|43113|4|Described|Table 1 p21||Ordovician|||||||
19210|Wairuna Formation|43213|5|Briefly described|p9, p66|Ordovician|Ordovician|Near Greenvale, Broken River Province. Quartzose flysch sediments, preserved as thrust slices.||||Faulted against the Precambrian Halls Reward Metamorphics.||
19210|Wairuna Formation|43253|5|Briefly described|map legend|Early Devonian|Ordovician|||||||
19210|Wairuna Formation|43259|4|Described|Appendix 1,p4.||Ordovician|||||||
19210|Wairuna Formation|43286|5|Briefly described|Map Legend|Early Devonian|Ordovician|||||||
19210|Wairuna Formation|43480|2|Defined|7 Fig.2|Devonian|Silurian|Age: 407Ma||||||03-AUG-20
19210|Wairuna Formation|43625|6|Mentioned|p20|||Age: Early-Middle Ordovician (probably)||||||
19210|Wairuna Formation|43716|6|Mentioned|p57|||||||||
19210|Wairuna Formation|43896|14|Not recorded|Map Legend||Early Silurian|||||||
19210|Wairuna Formation|43926|2|Defined|Tb.2,opp.10,map,p10,|||p20||||||
19210|Wairuna Formation|44044|2|Defined|p124-126,128||Llandoverian|Late Llandoverian graptolites. Includes Carriers Well Limestone and Everetts Creek Volcanic Members.||||||
19210|Wairuna Formation|44046|14|Not recorded|p150,Fig.21|||||||||
19210|Wairuna Formation|44048|14|Not recorded|Map Legend||Early Silurian|||||||
19210|Wairuna Formation|44049|14|Not recorded|Map Legend||Early Silurian|||||||
19210|Wairuna Formation|44050|14|Not recorded|p153,154,Pl.1|||||||||
19210|Wairuna Formation|44058|14|Not recorded|Table. p101|||||||||
19210|Wairuna Formation|44059|14|Not recorded|p442,443|Early Silurian|Late Ordovician|||||||
19210|Wairuna Formation|44061|4|Described|p10||Early Silurian|||||||
19210|Wairuna Formation|44091|14|Not recorded|p26,Tb.2,p28||Silurian|||||||
19210|Wairuna Formation|44359|14|Not recorded|Map Legend||Early Silurian|||||||
19210|Wairuna Formation|44515|2|Defined|p31-36||Silurian|Intruded by Gray Creek Complex. Complex relationship with other units. =Wairuna Beds.||||||
19210|Wairuna Formation|44516|14|Not recorded|p32,35|||||||||
19210|Wairuna Formation|45009|2|Defined|p21,26,40-3,45-6,50,||Early Silurian|p55,61,84,87,Pls. 13,15,Tb.6. Unconformably overlain by Graveyard Creek Formation. Intruded by Boiler Gully Complex and Herbert River Granite.||||||
19210|Wairuna Formation|45151|6|Mentioned|p7|||See also Table 3.||||||
19210|Wairuna Formation|48904|6|Mentioned|p17|||||||||
19210|Wairuna Formation|50202|5|Briefly described|Map legend|Ordovician|Ordovician|Mudstone, siltstone, quartzose arenite, chert and jasper.||||||
19210|Wairuna Formation|61727|5|Briefly described|p942 Fig.1|Ordovician|Ordovician|Informal name. Geological Province: Broken River Province/Graveyard Creek Subprovince.||||||
19210|Wairuna Formation|63154|5|Briefly described|p281 Fig. 3||Late Cambrian|Geological province: Broken River Province/Camel Creek Subprovince.||||||11-APR-07
19210|Wairuna Formation|67455|6|Mentioned|p576 Fig.2. |Ordovician|Ordovician|||||||
19210|Wairuna Formation|67848|5|Briefly described|p1, p2, p4, p5 Fig.3, pp6-16. |Late Silurian|Late Ordovician|Western edge of Camel Creek Subprovince. Volcanics. LA-ICPMS maximum depositional age of siliciclastic assemblage from detrital zircons. Part of an arc assemblage (volcanics) and accretionary wedge (sediments) in collisional accretion; a collage of rocks of different age and possibly tectonic setting. Strata disrupted by melange formation and island arc slices intercalated by thrusting in the late Devonian. Geochemistry, and web address for geochemical data, are given.|420.7 +/- 5.6 Ma (Henderson et al. 2011).||||Massive, aphyric, mafic to intermediate volcanic rocks; commonly amygdaloidal, rarely pillowed; lesser dacite and rhyolite; massive jasper and chert; quartz sandstone with siltstone and mudstone intervals, volcaniclastic sandstone.|05-MAY-15
19210|Wairuna Formation|68336|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician|Camel Creek Subprovince, Broken River Province.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange. Separately mapped are jasper and chert; quartzose sandstone, subordinate mudstone; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
19210|Wairuna Formation|68339|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician?|Camel Creek Subprovince.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange; minor altered aphyric tholeiitic basalt, locally pillowed.|
19210|Wairuna Formation|68340|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician?|Camel Creek Subprovince.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange; minor altered aphyric tholeiitic basalt, locally pillowed.|
19210|Wairuna Formation|68341|5|Briefly described|Map legend.|Early Silurian?|Late Ordovician|Camel Creek Subprovince, Broken River Province.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange. Separately mapped are jasper and chert; quartzose sandstone, subordinate mudstone; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
19210|Wairuna Formation|68344|5|Briefly described|Map legend.|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.|||||Mudstone, siltstone, quartzose arenite; local melange; jasper and chert mapped as a separate sub-unit.|
19210|Wairuna Formation|68478|5|Briefly described|Map Legend|Early Silurian|Ordovician|Camel Creek Subprovince.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange.|
19210|Wairuna Formation|68479|5|Briefly described|Map Legend|Early Silurian|Ordovician|Camel Creek Subprovince.|||||Mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange.|
19210|Wairuna Formation|68480|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. Late Ordovician? to Early Silurian? in age.|||||Undivided: mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange. Separately mapped are: jasper and chert; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
19210|Wairuna Formation|68481|5|Briefly described|Map Legend|Early Silurian|Late Ordovician|Camel Creek Subprovince. Late Ordovician? to Early Silurian? in age. The 3 facies are mapped separately.|||||Undivided: mudstone, siltstone, fine-grained quartzose sandstone, chert and jasper; local melange. Separately mapped are: jasper and chert; altered aphyric tholeiitic basalt, locally pillowed, minor chert and jasper.|
19210|Wairuna Formation|68553|6|Mentioned|Map legend; schematic diagram.|Silurian|Ordovician|Broken River Province. This unit, as well as Pelican Range Formation, Tribute Hills Arenite, Carriers Well Formation and Everetts Creek Volcanics, are all mapped under the symbol, OSb.||||||
19210|Wairuna Formation|68576|5|Briefly described|Q_11: p34-35, p37-39|||Greenvale area. Unfossiliferous: ages poorly known; may be Ordovician.|||||Quartzose turbidites: thin- to medium-bedded, fine- to medium-grained quartzose sandstone and mudstone. Complexly folded (at least two generations of folds) and locally disrupted.|
19210|Wairuna Formation|68731|5|Briefly described|p153 Fig 3.52|Silurian|Silurian|||||||18-JUL-14
19210|Wairuna Formation|68822|5|Briefly described|p335, p336 Fig.11|Upper Ordovician|Upper Ordovician||||||Mafic volcanics.|
19210|Wairuna Formation|69030|6|Mentioned|p6|Ordovician|Ordovician|Camel Creek Subprovince (Broken River Province).||||||
19210|Wairuna Formation|69079|6|Mentioned|p5|Ordovician|Ordovician|Camel Creek Subprovince, Broken River Province.||||||
19210|Wairuna Formation|69592|5|Briefly described|p250-252, p255, p268-270, p272, p277-279|Silurian|Silurian|See also p297. Camel Creek Subprovince, Broken River Province. A fault-bounded unit. No known fossils. Previously thought to be Ordovician (Withnall, 1993); middle to late Silurian ages from volcaniclastic sandstone and a felsic volcanic clast respectively.|433+/-4 Ma; 421+/-6 Ma (MDA: Henderson et al.2011)|||Adjacent to Greenvale Formation.|Cleaved mudstone and siltstone, fine-grained quartzose sandstone, altered basalt (aphyric and massive; locally amygdaloidal and pillowed) lenses to 4km long, chert and jasper. Contains sporadic fault-related serpentinite. Melange zones common.|
19210|Wairuna Formation|70207|6|Mentioned|p20|Silurian|Ordovician|Clarke River and/or Cairns region.||||||
19210|Wairuna Formation|70754|5|Briefly described|p461, p466-467, p470, p475, p479|Late Ordovician|Late Ordovician|Broken River region, 200km W of Townsville. Contains (inter alia) a brachiopod, Elliptoglossa, which also occurs in the Bowan Park area of central west NSW. Systematic palaeontological descriptions.||||||
19210|Wairuna Formation|71091|5|Briefly described|p146-147, p159, p164-165|||North Queensland. Limestones of this unit, previously referred to as the Carriers Well Formation, contain coral fauna resembling those in the Angullong Formation of NSW. See Zhen et al. (2015).||||||
19210|Wairuna Formation|73201|4|Described|p607, p610-618, p620|Late Ordovician|Middle Ordovician|Mossman Orogen, Broken River Province. Geochron are U-Pb LA-ICP-MS detrital zircon maximum depositional ages. These suggest deposition spanned much of the Middle to Late Ordovician and also supplant younger previous MDAs from Henderson et al. (2011). Detrital zircon provenance is linked to igneous rocks of the Macrossan and Pama Igneous associations. [See article for detailed lithologic and structural description, and detrital zircon provenance description]. Interleaved with the Greenvale Formation, Pelican Range Formation and Lucky Springs Assemblage.|465 +/- 2.4 Ma, 470 +/- 3.6 Ma, 453 +/- 2.9 Ma||||Quartzose greywacke with widespread melange and pre-slaty cleavage folding, common mafic volcanic bodies and chert lenses, and rare polymict conglomerate horizons.|
19212|Waite Formation|9199|5|Briefly described|Map legend|||Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|9394|5|Briefly described|Map Legend|Pliocene|Miocene|Siltstone, claystone, limestone (commonly silicified), sandstone.||||||
19212|Waite Formation|9694|5|Briefly described|Map Legend|Early Pliocene|Late Miocene|Chalcedonic limestone, red-brown sandstone, silty sandstone, clayey sandstone and sandy claystone.||||||
19212|Waite Formation|23844|6|Mentioned|p40|Cenozoic|Cenozoic|Chalcedonic limestone, sandstone, mudstone and sandy conglomerate. Equivalent to Mount Bleechmore Granulite on ALCOOTA||||||19-NOV-08
19212|Waite Formation|29673|6|Mentioned|p360|||||||||
19212|Waite Formation|30055|6|Mentioned|p153|||||||||
19212|Waite Formation|30582|6|Mentioned|p9|||Diprotodontid remains||||||
19212|Waite Formation|30638|6|Mentioned|p232|||Upper Miocene or Lower Pliocene||||||
19212|Waite Formation|33103|6|Mentioned|p15|||||||||
19212|Waite Formation|33104|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19212|Waite Formation|34996|6|Mentioned|p145|||||||||
19212|Waite Formation|36213|6|Mentioned|p89|||||||||
19212|Waite Formation|38371|6|Mentioned|p666|||||||||
19212|Waite Formation|39087|6|Mentioned|p16|||||||||
19212|Waite Formation|39610|4|Described|p8|||||||||
19212|Waite Formation|39898|5|Briefly described|Map legend|Tertiary|Tertiary|Greenish-grey siltstone, chalcedony and limestone.||||||14-FEB-06
19212|Waite Formation|40538|5|Briefly described|Map legend|early Pliocene|late Miocene|Chalcedonic limestone, grey; rare sandy mudstone.||||||15-NOV-05
19212|Waite Formation|40906|6|Mentioned|p30|||||||||
19212|Waite Formation|41537|6|Mentioned|Fig.2|||||||||
19212|Waite Formation|42375|5|Briefly described|Table 1 P11|||In the Waite Basin.||||||14-DEC-06
19212|Waite Formation|42420|6|Mentioned|p256|late Miocene||||||||
19212|Waite Formation|42457|6|Mentioned|p171|||||||||
19212|Waite Formation|42504|6|Mentioned|Table 1 P4|||||||||
19212|Waite Formation|42562|6|Mentioned|p95|||||||||
19212|Waite Formation|42776|5|Briefly described|p299|||||||||
19212|Waite Formation|43225|5|Briefly described|Map Legend||Tertiary|||||||
19212|Waite Formation|43503|5|Briefly described|45|||||||||
19212|Waite Formation|43565|3|Fully described|p422,431-440|Early Pliocene|Late Miocene|||||||
19212|Waite Formation|43748|4|Described|p8,19, Tb 1, p11,15,17|Early Pliocene|Late Miocene|Waite Basin. Includes vertebrate fossil assemblage. Middle unit within informal 'Alcoota beds' succession. 40m crops out. Full thickness not known. Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|||||Interbedded chalcedonic, calcarenitic limestone, sandstone, siltstone and minor sandy conglomerate.|19-DEC-11
19212|Waite Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|Geological Province: Waite Basin.||||||
19212|Waite Formation|44223|14|Not recorded|Fig.2|||Correlation of fauna.||||||
19212|Waite Formation|44227|14|Not recorded|p.59,74,91|Early Pliocene|Late Miocene|Alcoota fauna in early Pliocene or late Miocene. Diprotodontids. (F53-10).||||||
19212|Waite Formation|44238|14|Not recorded|Fig.3|Pliocene|Miocene|||||||
19212|Waite Formation|45028|2|Defined|p10-12|Pliocene|Miocene|See also Fig.2,4, p1,8,13-17,22,45,108,125,139,149,161,162,175,176,187. late Miocene or early Pliocene. (F53-10).||||||
19212|Waite Formation|45041|5|Briefly described|p118|||Mid Tertiary||||||
19212|Waite Formation|45128|6|Mentioned|p40|||||||||
19212|Waite Formation|46800|6|Mentioned|p109|||||||||
19212|Waite Formation|60547|5|Briefly described|Map Legend|Tertiary|Tertiary|Greenish and grey siltstone and mudstone; chalcedony in upper part.||||||
19212|Waite Formation|60551|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Waite Basin. Chalcedonic limestone.||||||
19212|Waite Formation|60668|5|Briefly described|Fig. 22a|||Chalcedonic limestone, sandstone, mudstone and conglomerate.||||||
19212|Waite Formation|60703|5|Briefly described|p704 Fig. 2, p725 Fig.18|Pliocene|Late Miocene|Geological Province: Waite Basin.||||||12-APR-05
19212|Waite Formation|61155|5|Briefly described|p5, p16|Late Miocene|Early Miocene|Lacustrine siltstones and chalcedonic limestones of central Australia. Age: >10Ma. Thickness: 20m. Geological Province: Hale, Ti-Tree and Waite  Basins.||||||07-OCT-15
19212|Waite Formation|61388|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Chalcedonic limestone, massive chalcedony.||||||19-NOV-08
19212|Waite Formation|61404|5|Briefly described|Map legend|Neogene|Paleogene|Limestone: chalcedonic; rare quartzic mudstone. Geological Province: southern Georgina Basin.||||||07-NOV-08
19212|Waite Formation|62082|5|Briefly described|p19, p52|Pliocene|Miocene|Forms caps on mesas where it is equivalent to Austral Downs Limestone and chert; often associated with duricrust. See also p53.||||||07-FEB-11
19212|Waite Formation|64068|3|Fully described|p80, 79, p42, p19|Pliocene|Miocene|Gastropods and vertebrates fossils. Overlies Cenozoic ferricrete. Is overlain by Quaternary alluvium. Lower part correlated with Poodyea Formation. Correlations: Austral Downs Limestone, Brunette Limestone, Arltunga beds.|||||Lacustrine green siltstone below fluviatile red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic chalcedonic limestone.|04-APR-12
19212|Waite Formation|65194|5|Briefly described|p53, p71-72, p74|Early Pliocene|Late Miocene|Waite Basin. Equivalents occur in Ti-Tree Basin which coarsen upwards, representing a change from lacustrine to fluvial conditions; overlain by undifferentiated Cenozoic alluvial sediments.||||||08-APR-16
19212|Waite Formation|65341|5|Briefly described|p2 Fig.2, p5, p19.|Cenozoic|Cenozoic|Waite Basin. Lacustrine and fluvial deposition. Outcrops as isolated low hills and in palaeochannels. Locally contains a gastropod and vertebrate fossil fauna indicating Late Miocene or Early Pliocene age.|||||Chalcedony, chalcedonic limestone, overlying lacustrine siltstone, fluviatile siltstone, sandstone and conglomerate.|
19212|Waite Formation|66131|6|Mentioned|p242 Fig.2|Miocene|Miocene|Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).||||||
19212|Waite Formation|69458|5|Briefly described|p42:7-13|||Waite Basin. Forms the hard resistant summit caps of many low plateaux and mesas. From lacustrine to fluvial deposits. Contains vertebrate fossils at the Alcoota fossil site (described).||Alcoota beds.||Unconformably overlies Tug Sandstone Member (Hale Formation).|Lacustrine green-grey siltstone, followed by fluvial red siltstone, sandstone and conglomeratic sandstone, capped by pedogenic cream or white, chalcedonic calcarenitic limestone.|12-JUL-16
19212|Waite Formation|72515|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Jervois Range Special Map Sheet. Waite Basin.||Alcoota beds|||Calcedonic limestone, calcite veins.|05-JUL-22
19212|Waite Formation|72516|3|Fully described|p11, p98|Pliocene|Miocene|Waite Basin. Type section occurs 6km south of Alcoota homestead. Intersected in drillhole BMR Alcoota 3. Outcrops as low plateaus and mesas peripheral to the margins of the Waite Basin on ALCOOTA and ALICE SPRINGS map sheets; equivalents are interpreted on HUCKITTA. Maximum thickness is >3m in the mapped area, 19-130m elsewhere. Deposited in a lacustrine or fluvial environment. Hosts late Miocene to early Pliocene verterbrate fossils. Interpreted to be an age correlative of the Austral Downs Limestone, Brunette Limestone and the Arltunga beds. Equivalents are interpreted in southern Huckitta.||Alcoota beds||Unconformably overlies the Denara Orthogneiss.|Chalcedonic limestone, calcite veins; recessive, lacustrine, green siltstone. Fluvial red silstone, sandstone, conglomeratic sandstone.|09-JUN-21
19228|Walford Dolomite|22453|6|Mentioned|p 12|||In the Mount Isa Basin.||||||14-DEC-06
19228|Walford Dolomite|22673|6|Mentioned|64,65,66|||||||||
19228|Walford Dolomite|22680|6|Mentioned|84,85|||Geological: province Mount Isa Basin. Of Fickling Group.||||||14-DEC-06
19228|Walford Dolomite|23031|6|Mentioned|27|||Of the Fickling Group.||||||21-SEP-06
19228|Walford Dolomite|23065|6|Mentioned|16|||Geological province: Lawn Hill Subprovince. Of the Fickling Group. Underlain by Fish River Formation.||||||14-DEC-06
19228|Walford Dolomite|23393|5|Briefly described|p20|Paleoproterozoic|Paleoproterozoic|Of Fickling Group.||||||07-NOV-08
19228|Walford Dolomite|23396|5|Briefly described|p407 Fig.2|||Of Fickling Group.||||||21-SEP-06
19228|Walford Dolomite|23398|4|Described|p445|Statherian|Statherian|Age: 1649+/-7Ma.||||||21-SEP-06
19228|Walford Dolomite|23406|4|Described|p611, p609 Fig. 9|Statherian|Statherian|Of Fickling Group. Age: 1649+/-7Ma. Geological province: Murphy Inlier. Included in the Loretta Supersequence.  Lithological details included in Fig. 9.||||||16-JUN-09
19228|Walford Dolomite|23466|5|Briefly described|p269|||||||||
19228|Walford Dolomite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Fickling Group.   Geological Province:  Mount Isa Superbasin||||||07-NOV-08
19228|Walford Dolomite|24432|4|Described|p565 Fig.2, p566 Fig.5|Statherian|Statherian|Age: <1649+/-7 Ma. Overlain by Mount Les Siltstone. Geological Province: Lawn Hill Platform.||||||
19228|Walford Dolomite|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|36012|3|Fully described|Table 3|||See also p16.||||||21-SEP-06
19228|Walford Dolomite|36217|6|Mentioned|p206|||Published by Grimes and others 1979. Definition approved by Qld SNC.||||||21-SEP-06
19228|Walford Dolomite|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|38237|6|Mentioned|p128|||||||||
19228|Walford Dolomite|38348|6|Mentioned|p11|||||||||
19228|Walford Dolomite|38584|4|Described|p17|||||||||
19228|Walford Dolomite|39445|5|Briefly described|Table 2|||See also p39.||||||21-SEP-06
19228|Walford Dolomite|39497|6|Mentioned|Fig.4|||||||||
19228|Walford Dolomite|39685|6|Mentioned|p407|||||||||
19228|Walford Dolomite|39925|6|Mentioned|Fig.9|||||||||
19228|Walford Dolomite|39944|6|Mentioned|Fig.5|||||||||
19228|Walford Dolomite|41721|4|Described|p28|||||||||
19228|Walford Dolomite|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
19228|Walford Dolomite|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Fickling Group. Of "Mid Proterozoic" age.||||||21-SEP-06
19228|Walford Dolomite|45162|6|Mentioned|p146|||||||||
19228|Walford Dolomite|45166|5|Briefly described|p30|||||||||
19228|Walford Dolomite|49001|2|Defined|p9|Carpentarian|Carpentarian|||||||
19228|Walford Dolomite|60558|5|Briefly described|p5 Fig. 4|||Of Fickling Group. Includes Basal Member. Overlain by Mount Les Siltstone, underlain by Fish River Formation.||||||
19228|Walford Dolomite|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1649+/-7Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier, Isa Superbasin.||||||07-NOV-08
19228|Walford Dolomite|63111|5|Briefly described|p1164 Tb. 1, p1163 Fig. 3|Statherian|Statherian|Of Loretta Supersequence. Age: 1647+/-4Ma and 1649+/-7Ma. Geological Province: Isa Superbasin. Laminated fine-grained sandstone and siltstones, peloid-dolograinstones, dolomudstone and carbonates.||||||07-FEB-11
19228|Walford Dolomite|63113|5|Briefly described|p1211, p1216, p1225-1226; Figs.2,13.  |||Minerals associated with residual hydrocarbons were predominantly pyrite and elemental (?native) Zn, Cu and Ag; native Pb in veinlets and native Ni dispersed throughout the organic matrix. Appears as Walford Ck. Dolomite in Fig.13. Part of Loretta supersequence. Source of hydrocarbons in this unit was probably Mount Les Siltstone.||Of the Loretta supersequence||Is overlain by Mount Les Siltstone.||
19228|Walford Dolomite|63866|5|Briefly described|p56|Statherian|Statherian|Isa Superbasin.|1649 +/- 7 Ma (depositional age)|||Equivalent to the Loretta Supersequence.||
19228|Walford Dolomite|65228|5|Briefly described|p26, Fig.04.|Statherian|Statherian|Part of Loretta Supersequence.|1649 +/- 7 Ma (SHRIMP).|||||
19228|Walford Dolomite|65337|6|Mentioned|p30, p36.|||||Unit in Fickling Group.||||
19228|Walford Dolomite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Isa Superbasin.|1649 +/- 7 Ma (maximum depositional age).|Fickling Group.|||Blocky grey oolitic, stromatolitic and intraclastic dolomite; minor dolomitic sandstone and shale.|
19228|Walford Dolomite|69591|5|Briefly described|p42, p43 Fig.2.31, p55|||Camooweal-Murphy Domain, Isa Superbasin. Part of Loretta Supersequence. Peritidal deposits.|1649 +/- 7 Ma (MDA: Page et al., 2000).|Fickling Group.|||Blocky grey oolitic, stromatolitic and intraclastic dolomite; minor dolomitic sandstone and shale.|
19228|Walford Dolomite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1649+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuff.|
19228|Walford Dolomite|72526|5|Briefly described|p8 Fig.1.3, p20.|Statherian|Statherian|Shown as being located in the central and west of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1649 +/-7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone.||
19228|Walford Dolomite|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Statherian|Statherian|Located in the West and Central of the South Nicholson Basin. U-Pb zircon sedimentary depositional age given.|1644 +/- 7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone. Partially laterally equivalent with Bullrush Conglomerate and Shady Bore Quartzite.|Includes dolomitic siltstone.|
19228|Walford Dolomite|72913|5|Briefly described|p7 Fig.2.|Paleoproterozoic|Paleoproterozoic|Shown as being in the central part of the Isa Superbasin. See also Walford Dolostone, discussed in text.|1649 +/- 7 Ma|Fickling Group||Overlies Fish River Formation and underlies Mount Les Siltstone.|Includes dolomitic siltstone.|
19228|Walford Dolomite|73042|6|Mentioned|p4, p14, p17|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1649 +/- 7 Ma|Fickling Group||Underlain by Fish River Formation. Conformably overlain by Mount Les Siltstone.||
19247|Wall Sandstone Member|22593|6|Mentioned|Table 1|||||||||
19247|Wall Sandstone Member|23161|4|Described|p28|Early Permian|Early Permian|||||||
19247|Wall Sandstone Member|32945|6|Mentioned|p79|||Permian. Gebbie Fm. See also P80.||||||
19247|Wall Sandstone Member|32949|5|Briefly described|p441|||||||||
19247|Wall Sandstone Member|36739|6|Mentioned|p13|||||||||
19247|Wall Sandstone Member|37071|6|Mentioned|p84|||||||||
19247|Wall Sandstone Member|38917|6|Mentioned|p155|||||||||
19247|Wall Sandstone Member|39267|6|Mentioned|p232|||||||||
19247|Wall Sandstone Member|39423|6|Mentioned|p54|||||||||
19247|Wall Sandstone Member|40571|6|Mentioned|p31|||||||||
19247|Wall Sandstone Member|41034|4|Described|p374|||||||||
19247|Wall Sandstone Member|42257|5|Briefly described|Table 1 P263|||||||||
19247|Wall Sandstone Member|43475|14|Not recorded|p553||Permian|||||||
19247|Wall Sandstone Member|43882|14|Not recorded|p94|||(Nebo)||||||
19247|Wall Sandstone Member|44000|2|Defined|Tb.1,p26,32-34,Pl.6|||Member of Gebbie Formation near base.Lower Permian rare marine fossils.||||||
19247|Wall Sandstone Member|45071|4|Described|p48|||||||||
19247|Wall Sandstone Member|48847|14|Not recorded|p3,5-7,9|||Marker horizon. Below base of Collinsville Coal Measures.||||||
19247|Wall Sandstone Member|48881|14|Not recorded|p22|||||||||
19247|Wall Sandstone Member|65388|5|Briefly described|p186, 187, 188|||Near base of Gebbie Formation, Bowen Basin. Base suggested as readily mappable boundary between Tiverton Formation and base of Gebbie Formation by Waterhouse & Jell (1983, page 232), but current lower boundary based on Jensen & others (1966) and Bowen Basin Solid Geology Map (Geological Survey of Queensland, 1988) . This member not distinguished in current mapping.||||||09-SEP-14
19254|Wallaby beds|32945|6|Mentioned|p88|||Permian||||||
19254|Wallaby beds|43475|14|Not recorded|p553||Permian|See also Lexicon||||||
19254|Wallaby beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, lithic arenite, and locally ferruginous siltstone.||||||
19254|Wallaby beds|63748|4|Described|p7 Fig. 3, p19|Permian|Permian|Unconformably overlies the Eurydesma beds; unconformably overlain by Eight Mile Creek beds. Thickness: ~150m. Consists of a lower sequence of conglomerate, lithic arenite and siltstone overlain by an upper sequence of mainly ferruginous siltstone.||||||07-FEB-11
19254|Wallaby beds|68679|5|Briefly described|p446, p452|Permian|Permian|Silver Spur Subprovince, Woolomin Province. ~150m thick.||Wildash Group.||Unconformably overlies the Eurydesma beds. Is overlain unconformably by Eight Mile Creek beds. Is downfaulted against the Silverwood Group.|Conglomerate, lithic sandstone and siltstone overlain by mainly ferruginous siltstone. Contains abundant marine and plant fossils.|
19265|Wallangarra Volcanics|22857|5|Briefly described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Group. Rhyolitic and rhyodacitic flows and tuffs. Max. thickness: 450m. Geological Province: New England Fold Belt.||||||
19265|Wallangarra Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Ignimbrite rhyolite and rhyodacite and lesser rhyolitic lavas, including bedded epiclastic tuffs.||||||27-SEP-18
19265|Wallangarra Volcanics|23812|5|Briefly described|p28 Tb.3, p25|Late Permian|Early Permian|Of Wandsworth Volcanic Group.  Maximum thickness: 450m.||||||12-AUG-08
19265|Wallangarra Volcanics|23859|5|Briefly described|p930|Late Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
19265|Wallangarra Volcanics|31694|6|Mentioned|p350|||||||||
19265|Wallangarra Volcanics|38824|6|Mentioned|p215|||||||||
19265|Wallangarra Volcanics|39252|6|Mentioned|p28|||See also Fig.15||||||
19265|Wallangarra Volcanics|39445|6|Mentioned|Fig.8|||||||||
19265|Wallangarra Volcanics|40509|6|Mentioned|p47|||||||||
19265|Wallangarra Volcanics|42378|5|Briefly described|Table 1 p8|||||||||27-SEP-18
19265|Wallangarra Volcanics|42559|4|Described|p10|||Stated to be informal name.||||||
19265|Wallangarra Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
19265|Wallangarra Volcanics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
19265|Wallangarra Volcanics|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Dacitic to rhyolitic ignimbrite, strongly welded and moderately to very crystal-rich - numerous fragments of andesine, biotite, orthoclase, quartz.  Welded ignimbrite with fragments of orthoclase, oligoclase, quartz and minor biotite.||||||11-DEC-07
19265|Wallangarra Volcanics|63748|4|Described|p19, p36, p69|Late Permian|Late Permian|Unconformable on Texas beds; intruded by Stanthorpe Granite and possibly by Undercliffe Falls Granite. Max.thickness: 450m. Geol.prov: Wandsworth Province. Rhyolitic and rhyodacitic tuffs and lavas with possible epiclastic interbeds. Detailed lithology.||||||27-SEP-18
19265|Wallangarra Volcanics|65668|5|Briefly described|p2 Tb.1, p31-34|Permian|Permian|Stanthorpe area. Considered to be closely related to Emmaville Volcanics; both units placed in Wandsworth Volcanic Group by Barnes et al. (1991). Age: 253 +/- 2.4 Ma (SHRIMP U-Pb zircon). A 300-450 m thick sequence of rhyolitic to rhyodacitic ignimbrites and lavas. Is intruded by Stanthorpe Granite; is overlain by Dundee Rhyodacite.||||||
19265|Wallangarra Volcanics|68005|5|Briefly described|pp151-152.|Permian|Permian|||Unit in Wandsworth Volcanic Group.|||Ignimbritic rhyolite and rhyodacite and lesser rhyolitic lavas. Includes bedded epiclastic tuffs.|
19265|Wallangarra Volcanics|68111|5|Briefly described|p968 Tb.1|Olenekian|Wuchiapingian||253 +/- 2.4 Ma, U-Pb SHRIMP (Cross et al. 2009).|Of the Wandsworth Volcanic Group.||||
19265|Wallangarra Volcanics|68679|4|Described|p453, p455-458|Permian|Permian|Simmonds (1958) and several others listed. Stroud et al. (1992) included the unit in the Wandsworth Volcanic Group and equated it with the Emmaville Volcanics. Wandsworth Province. Crops out in the NSW-QLD border area between Ballandean and Wallangarra. 300-450m thick. High-K calc-alkaline. Represents eruption of a large silicic magma system. Is equated with the Emmaville Volcanics.|253 +/- 2.4 Ma (SHRIMP U-Pb: Cross et al., 2009).|Wandsworth Volcanic Group.||Unconformably overlies Texas beds. Is overlain unconformably by Dundee Rhyolite. Is intruded by Stanthorpe, Dormans Flat, Sailor Jack Granites and possibly the Bungulla Monzogranite.|Rhyolitic and rhyodacitic tuff and lava with possible epiclastic interbeds. Later decribed as two thick intracaldera ignimbrite units separated by <50m package of thinly bedded ignimbrite, air fall deposits, surge deposits and epiclastic sediments.|
19265|Wallangarra Volcanics|68901|5|Briefly described|p6, p8, p129|Late Permian|Late Permian|Age from Cross et al., 2009.
|253+/-2.4 Ma SHRIMP,|||||27-SEP-18
19265|Wallangarra Volcanics|69639|5|Briefly described|p220|||See also Wallangara Volcanics p44, p62.|235.0 +/- 2.4 Ma|Wandsworth Volcanic Group||Unconformably overlies the Texas Beds.||
19265|Wallangarra Volcanics|70876|5|Briefly described|p82|Late Permian|Late Permian||253 +/- 2.4 Ma (Cross et al, 2009).|Wandsworth Volcanic Group||Overlies the Drake Volcanics. Overlain by the Emmaville Volcanics.||
19265|Wallangarra Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|253+/-2.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
19265|Wallangarra Volcanics|71628|5|Briefly described|p11-11; p12: 3, 5-6, 13; p15: 33, 40|Permian|Permian|See also p15: 57, 65, 75, 82-83, 97; p19: 6, 8, 160. RELATED UNITS (continued): Is also intruded by Severn River Monzogranite; Mount Norman Leucomonzogranite; Ruby Creek Leucogranite; Tenterfield Creek Leucosyenogranite; Stanthorpe Complex.||Wandsworth Volcanic Group.||Unconformably overlies Ballandean Monzogranite. Is intruded by Bungulla, Accommodation Creek, Blacksmiths Creek, Dormans Flat, Sailor Jack, Mount Lindesay Monzogranites. See COMMENTS for more.||
19265|Wallangarra Volcanics|71701|5|Briefly described|p170|Lopingian|Lopingian||253.8 +/- 2.4 Ma  (SHRIMP, Cross et al, 2009)|||||
19275|Wallaroo Basalt|23423|5|Briefly described|p262||Cenozoic|Atherton Subprovince.||||||19-NOV-08
19275|Wallaroo Basalt|23503|5|Briefly described|Map Legend||Miocene|||||||
19275|Wallaroo Basalt|24475|6|Mentioned|p50|||Not related to Wallaroo Group (SA).||||||
19275|Wallaroo Basalt|34046|6|Mentioned|Table III|||||||||
19275|Wallaroo Basalt|39445|5|Briefly described|Table 14|||||||||
19275|Wallaroo Basalt|43926|14|Not recorded|Tb.2,opp.p10,18|||||||||
19275|Wallaroo Basalt|45009|2|Defined|p96|||Contains equivalents of Older and Newer McBride Basalts.||||||
19275|Wallaroo Basalt|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as parts of the McBride and Nulla Basalt Groups; the Atherton, Chudleigh, McIvor River, McLean, Piebald\ and Sturgeon Basalts, and unnamed basalt flows, are all mapped under the symbol, TQbn.||||||
19275|Wallaroo Basalt|69599|5|Briefly described|p642|||Wallaroo volcanic field, 50km S of the Atherton Province. Four volcanic centres; flows down the former Herbert River.|10.3-6 Ma (Stephenson et al., 1980).||||Mostly alkali basalt.|
19303|Walloon Coal Measures|12597|3|Fully described|p489, p491, p493 Fig.2, p496, p501-508|Middle Jurassic|Middle Jurassic|Clarence-Moreton and Surat Basins. Upgraded to Subgroup status in NE part of Clarence-Moreton Basin (Jones and Patrick, 1981). Known as Walloon Subgroup in Surat Basin. Unique high-volatile and perhydrous coal, suitable for synthetic fuels. Thickness to 600m. Type section in the Rosewood area (Cameron, 1970). Coal described in detail.|||Includes Taroom Coal Measures, Tangalooma Sandstone and Juandah Coal Measures.|Overlies Bundamba Group.|Lithic and feldspathic sandstones interbedded with siltstone, mudstone, carbonaceous shale and coal.|
19303|Walloon Coal Measures|13497|6|Mentioned|p142 |||Surat Basin.||||||
19303|Walloon Coal Measures|13516|6|Mentioned|p166, p167 fig 10, p173|Jurassic|Jurassic|In Surat Basin, Eromanga Basin.||||||
19303|Walloon Coal Measures|22757|5|Briefly described|p7|||Also Table6,p11. Surat Basin. 635 m.||||||
19303|Walloon Coal Measures|22820|6|Mentioned|p31 Fig. 11|Cretaceous|Jurassic|||||||
19303|Walloon Coal Measures|22857|4|Described|p295, p314-5, p546 App.1 Tb.A1.12|Late Jurassic|Middle Jurassic|Of Injune Creek Gp. Interbedded sst, sltst, claystone, coal, ironstone nodules. Contains significant coal deposits in Qld. Overlies Bundamba Gp; unconformably underlies Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Surat Basin. See p312-3 Fig.22.6||||||
19303|Walloon Coal Measures|22865|3|Fully described|p295,314,318|Bathonian|Middle Jurassic|||||||
19303|Walloon Coal Measures|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|23036|4|Described|6|||Max thickness: 700 m.||||||11-DEC-07
19303|Walloon Coal Measures|23050|4|Described|p23 Table 4|Late Jurassic|Middle Jurassic|Of Surat Basin. Age: palynology data indicates a J4 Jurassic age.||||||11-DEC-07
19303|Walloon Coal Measures|23051|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|of Surat Basin.||||||
19303|Walloon Coal Measures|23053|6|Mentioned|Fig10p17|Callovian|Aalenian|||||||
19303|Walloon Coal Measures|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19303|Walloon Coal Measures|23375|6|Mentioned|p278|||of Surat Basin.||||||
19303|Walloon Coal Measures|23720|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|Grey claystone, lithic sandstone (arenites and wackes), coal.  Includes Towallum Basalt (basalt, minor basalt breccia) at the base.||||||15-DEC-04
19303|Walloon Coal Measures|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
19303|Walloon Coal Measures|23799|4|Described|p49, p10 Tb. 1, p48 Fig. 3|Callovian|Bathonian|Supersedes Walloon beds (Cameron, 1907).   Correlated w Injune Creek Group. Unconformably overlain by Main Range Volcanics.  Max. thickness: 600m.  Type Section: in drillhole N.S.84, Ebenezer district. Geol. Prov: Clarence-Moreton Basin (also Surat Basin)||||||28-SEP-05
19303|Walloon Coal Measures|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
19303|Walloon Coal Measures|23811|5|Briefly described|Map Legend|Callovian|Bajocian|Thin-bedded, claystone, lithic and sublithic to feldspathic arenites, coal seams and partings; ironstone nodules and thin beds.  Includes Maclean Sandstone Member at top.Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
19303|Walloon Coal Measures|23812|4|Described|p36, p34 Tb.4|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone, underlain by Bundamba Group.  Geological Province: Clarence-Moreton Basin.  Maximum thickness: 400m.||||||11-DEC-07
19303|Walloon Coal Measures|23818|6|Mentioned|p140|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
19303|Walloon Coal Measures|23843|4|Described|p455|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 600m.||||||
19303|Walloon Coal Measures|23888|6|Mentioned|p262|||||||||
19303|Walloon Coal Measures|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|24068|4|Described|p270 Table 2|Middle Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 520m.||||||
19303|Walloon Coal Measures|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
19303|Walloon Coal Measures|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|24127|5|Briefly described|p5|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24129|5|Briefly described|p4|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24159|5|Briefly described|p148 Fig. 2, p152|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin. Overlying Unit: Pilliga Sandstone. Underlying Unit: Hutton Sandstone.||||||
19303|Walloon Coal Measures|24160|6|Mentioned|p18|||Upper coal sequence produces bentonite as a byproduct.||||||
19303|Walloon Coal Measures|24225|5|Briefly described|p381|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|24237|5|Briefly described|p5 Fig.1|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
19303|Walloon Coal Measures|24299|5|Briefly described|p3|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24616|6|Mentioned|p35, p36, p37|||Geological Province: Clarence-Moreton and Surat Basins.||||||
19303|Walloon Coal Measures|29385|6|Mentioned|p82|||Jurassic.||||||
19303|Walloon Coal Measures|29393|6|Mentioned|p10|||Triassic.||||||
19303|Walloon Coal Measures|29591|6|Mentioned|p83|||||||||
19303|Walloon Coal Measures|29720|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|29869|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|29870|6|Mentioned|p15|||||||||
19303|Walloon Coal Measures|30024|6|Mentioned|p332|||||||||
19303|Walloon Coal Measures|30058|4|Described|p5|||See also p6-9. Jurassic age. type section illustrated p8. Is  the interval from 24ft 6 inches to 772ft in diamond drillhole N.S. 84 situated in the Ebenezer district. hole was drilled by the Department of Mines. Further description of location given, and shown on Fig.24, Fig. 25.||||||20-FEB-19
19303|Walloon Coal Measures|30131|6|Mentioned|p10|||See also P8||||||
19303|Walloon Coal Measures|30133|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|30455|6|Mentioned|p17|||See also P21. Jurassic age||||||
19303|Walloon Coal Measures|30457|6|Mentioned|p96|||||||||
19303|Walloon Coal Measures|30458|6|Mentioned|p3|||Jurassic age||||||
19303|Walloon Coal Measures|30460|6|Mentioned|p15|||See also P22. Jurassic age||||||
19303|Walloon Coal Measures|30463|6|Mentioned|p464|||Jurassic age||||||
19303|Walloon Coal Measures|30464|6|Mentioned|Fig.1|||Jurassic||||||
19303|Walloon Coal Measures|30465|6|Mentioned|p4|||||||||
19303|Walloon Coal Measures|30466|6|Mentioned|Fig.1|||Jurassic age||||||
19303|Walloon Coal Measures|30471|6|Mentioned|p131|||||||||
19303|Walloon Coal Measures|30475|6|Mentioned|p159|||||||||
19303|Walloon Coal Measures|30610|6|Mentioned|p326|||Refers Chesnut (1968) Hind & Helby (1969),Wallis (1968)||||||
19303|Walloon Coal Measures|30687|5|Briefly described|p63|||Middle-Upper Jurassic age. See also P65||||||
19303|Walloon Coal Measures|30692|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|30695|6|Mentioned|p3|||||||||
19303|Walloon Coal Measures|30699|6|Mentioned|p52|||See also P53. Stratigraphy. Map||||||
19303|Walloon Coal Measures|30701|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19303|Walloon Coal Measures|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19303|Walloon Coal Measures|30785|6|Mentioned|p397|||||||||
19303|Walloon Coal Measures|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|31086|6|Mentioned|p38|||? Mid Jurassic to ? Upper Jurassic age.||||||
19303|Walloon Coal Measures|31117|6|Mentioned|p379|||||||||
19303|Walloon Coal Measures|31118|4|Described|p322|||||||||
19303|Walloon Coal Measures|31132|6|Mentioned|p148|||||||||
19303|Walloon Coal Measures|31560|6|Mentioned|p630|||||||||
19303|Walloon Coal Measures|31563|6|Mentioned|p144|||||||||
19303|Walloon Coal Measures|32136|6|Mentioned|p5|||Miospores||||||
19303|Walloon Coal Measures|32137|6|Mentioned|p355|||||||||
19303|Walloon Coal Measures|32276|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.M - U||||||
19303|Walloon Coal Measures|32413|6|Mentioned|p86|||||||||
19303|Walloon Coal Measures|32492|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19303|Walloon Coal Measures|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|32913|6|Mentioned|p393|||Stratigraphy||||||
19303|Walloon Coal Measures|32916|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|32920|6|Mentioned|p89|||||||||
19303|Walloon Coal Measures|32924|6|Mentioned|p112|||||||||
19303|Walloon Coal Measures|32990|6|Mentioned|p81|||||||||
19303|Walloon Coal Measures|33075|6|Mentioned|Table 1|||Refers Whitehouse (1954)||||||
19303|Walloon Coal Measures|33091|5|Briefly described|p10|||Stratigraphy||||||
19303|Walloon Coal Measures|33128|6|Mentioned|Fig.11|||||||||
19303|Walloon Coal Measures|33367|3|Fully described|p17|||Equiv.Birkhead Fm.||||||
19303|Walloon Coal Measures|33368|6|Mentioned|p17|||Oil shale seams.||||||
19303|Walloon Coal Measures|33371|4|Described|p58|||Equiv. Birkhead Fm.||||||
19303|Walloon Coal Measures|33381|3|Fully described|p110|||Jur. Map. See also pp117,119,120 and 123.||||||11-DEC-07
19303|Walloon Coal Measures|33476|4|Described|p104|||Mention Fig.10||||||
19303|Walloon Coal Measures|33672|6|Mentioned|p44|||||||||
19303|Walloon Coal Measures|33709|6|Mentioned|p100|||Jurassic.||||||
19303|Walloon Coal Measures|33766|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|33774|6|Mentioned|p54|||Correlation||||||
19303|Walloon Coal Measures|33828|6|Mentioned|Table 3|||||||||
19303|Walloon Coal Measures|33939|6|Mentioned|p393|||Jurassic.  Flora.||||||
19303|Walloon Coal Measures|33971|6|Mentioned|p36|||See also Fig.29.||||||
19303|Walloon Coal Measures|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
19303|Walloon Coal Measures|34254|6|Mentioned|p489|||Jurassic||||||
19303|Walloon Coal Measures|34287|6|Mentioned|p171|||Jurassic. See also PP173,175||||||
19303|Walloon Coal Measures|34340|3|Fully described|p469|||||||||
19303|Walloon Coal Measures|34400|5|Briefly described|p13|||||||||
19303|Walloon Coal Measures|34452|6|Mentioned|p7|||See also PP12,13||||||
19303|Walloon Coal Measures|34540|6|Mentioned|p65|||Middle Jurassic||||||
19303|Walloon Coal Measures|34593|6|Mentioned|p539|||Jurassic||||||
19303|Walloon Coal Measures|34611|6|Mentioned|p140|||Jurassic||||||
19303|Walloon Coal Measures|34755|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|34881|6|Mentioned|p526|||||||||
19303|Walloon Coal Measures|34905|6|Mentioned|p530|||||||||
19303|Walloon Coal Measures|34950|5|Briefly described|p40|||||||||
19303|Walloon Coal Measures|35016|6|Mentioned|p41|||||||||
19303|Walloon Coal Measures|35053|5|Briefly described|p36|||||||||
19303|Walloon Coal Measures|35065|6|Mentioned|p45|||||||||
19303|Walloon Coal Measures|35101|6|Mentioned|p56|||||||||
19303|Walloon Coal Measures|35126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19303|Walloon Coal Measures|35156|4|Described|p7|||See also Table.2||||||
19303|Walloon Coal Measures|35157|6|Mentioned|p525|||||||||
19303|Walloon Coal Measures|35435|6|Mentioned|p43|||||||||
19303|Walloon Coal Measures|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
19303|Walloon Coal Measures|35648|6|Mentioned|p16|||||||||
19303|Walloon Coal Measures|35663|6|Mentioned|p129|||||||||
19303|Walloon Coal Measures|35811|5|Briefly described|Table 5|||||||||
19303|Walloon Coal Measures|35866|6|Mentioned|p403|||||||||
19303|Walloon Coal Measures|35937|6|Mentioned|p621|||||||||
19303|Walloon Coal Measures|36172|6|Mentioned|Appendix|||||||||
19303|Walloon Coal Measures|36243|6|Mentioned|Table 7A|||||||||
19303|Walloon Coal Measures|36327|6|Mentioned|p7|||||||||
19303|Walloon Coal Measures|36354|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|36570|2|Defined|p34|Jurassic|Jurassic|See also p25 and Fig.9, p55.||||||04-JUN-07
19303|Walloon Coal Measures|36574|6|Mentioned|p599|||||||||
19303|Walloon Coal Measures|36579|6|Mentioned|p447|||||||||
19303|Walloon Coal Measures|36779|4|Described|p7|||||||||
19303|Walloon Coal Measures|36939|6|Mentioned|p218|||||||||
19303|Walloon Coal Measures|36961|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|37065|5|Briefly described|p38|||||||||
19303|Walloon Coal Measures|37114|6|Mentioned|p308|||||||||
19303|Walloon Coal Measures|37116|6|Mentioned|p310|||||||||
19303|Walloon Coal Measures|37117|4|Described|p313|||||||||
19303|Walloon Coal Measures|37118|6|Mentioned|p318|||||||||
19303|Walloon Coal Measures|37122|4|Described|p328, p331|||||||||
19303|Walloon Coal Measures|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|37375|4|Described|p473|||||||||
19303|Walloon Coal Measures|37436|6|Mentioned|p540|||||||||
19303|Walloon Coal Measures|37463|6|Mentioned|p479|||||||||
19303|Walloon Coal Measures|37856|6|Mentioned|Table 3|||||||||
19303|Walloon Coal Measures|37988|6|Mentioned|p209|||||||||
19303|Walloon Coal Measures|37991|6|Mentioned|p179|||||||||
19303|Walloon Coal Measures|37992|4|Described|p165|||||||||
19303|Walloon Coal Measures|37993|6|Mentioned|p153|||||||||
19303|Walloon Coal Measures|37994|5|Briefly described|p143|||||||||
19303|Walloon Coal Measures|37995|4|Described|p64|||||||||
19303|Walloon Coal Measures|37997|6|Mentioned|p83|||||||||
19303|Walloon Coal Measures|38064|5|Briefly described|p41|||||||||
19303|Walloon Coal Measures|38068|6|Mentioned|p71|||||||||
19303|Walloon Coal Measures|38074|5|Briefly described|Table 1|||||||||
19303|Walloon Coal Measures|38079|6|Mentioned|p46|||||||||
19303|Walloon Coal Measures|38080|6|Mentioned|p54|||||||||
19303|Walloon Coal Measures|38205|2|Defined|p86|Jurassic|Jurassic|Previously "Walloon Beds".||||||04-JUN-07
19303|Walloon Coal Measures|38391|6|Mentioned|p11|||||||||
19303|Walloon Coal Measures|38441|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|Early to Middle JurassicE - M||||||
19303|Walloon Coal Measures|38741|5|Briefly described|p337|||||||||
19303|Walloon Coal Measures|39071|6|Mentioned|p339|||||||||
19303|Walloon Coal Measures|39212|5|Briefly described|p16|||See also P22||||||
19303|Walloon Coal Measures|39218|6|Mentioned|p48|||Flora||||||
19303|Walloon Coal Measures|39413|6|Mentioned|p53|||||||||
19303|Walloon Coal Measures|39445|5|Briefly described|Table 10|||See also Fig.8||||||
19303|Walloon Coal Measures|39494|6|Mentioned|Fig.5|||||||||
19303|Walloon Coal Measures|39642|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|39666|6|Mentioned|p113|||||||||
19303|Walloon Coal Measures|39708|6|Mentioned|p477|||||||||
19303|Walloon Coal Measures|39757|6|Mentioned|p1601|||||||||
19303|Walloon Coal Measures|39907|4|Described|p16|||||||||
19303|Walloon Coal Measures|39941|6|Mentioned|p471|||||||||
19303|Walloon Coal Measures|39942|6|Mentioned|p465|||||||||
19303|Walloon Coal Measures|39943|6|Mentioned|Table 9A|||||||||
19303|Walloon Coal Measures|39969|6|Mentioned|p11|||||||||
19303|Walloon Coal Measures|39988|6|Mentioned|p288|||||||||
19303|Walloon Coal Measures|40030|6|Mentioned|Fig.5|||||||||
19303|Walloon Coal Measures|40245|6|Mentioned|Table 1|||See also Table 2||||||
19303|Walloon Coal Measures|40249|6|Mentioned|p38|||||||||
19303|Walloon Coal Measures|40250|6|Mentioned|p35|||||||||
19303|Walloon Coal Measures|40540|6|Mentioned|p150|||||||||
19303|Walloon Coal Measures|40544|6|Mentioned|Fig.6|||||||||
19303|Walloon Coal Measures|40623|5|Briefly described|p30|||||||||
19303|Walloon Coal Measures|40767|6|Mentioned|p14|||||||||
19303|Walloon Coal Measures|40780|4|Described|p6|||||||||
19303|Walloon Coal Measures|40896|6|Mentioned|p51|||||||||
19303|Walloon Coal Measures|40926|6|Mentioned|Table 2|||||||||
19303|Walloon Coal Measures|40953|4|Described|p19|||||||||
19303|Walloon Coal Measures|41060|5|Briefly described|p2|||Generalized stratigraphy||||||
19303|Walloon Coal Measures|41122|6|Mentioned|p201|||||||||
19303|Walloon Coal Measures|41175|6|Mentioned|p195|||||||||
19303|Walloon Coal Measures|41176|6|Mentioned|p206|||||||||
19303|Walloon Coal Measures|41187|6|Mentioned|p217|||||||||
19303|Walloon Coal Measures|41188|6|Mentioned|Fig.3|||||||||
19303|Walloon Coal Measures|41210|6|Mentioned|p164|||||||||
19303|Walloon Coal Measures|41216|6|Mentioned|p300|||See also Fig.18||||||
19303|Walloon Coal Measures|41247|6|Mentioned|Fig.7|||||||||
19303|Walloon Coal Measures|41266|6|Mentioned|Fig.3|||||||||
19303|Walloon Coal Measures|41290|6|Mentioned|p226|||||||||
19303|Walloon Coal Measures|41591|6|Mentioned|p17|||See also Fig.2||||||
19303|Walloon Coal Measures|41631|4|Described|p20|||See also Fig.2||||||
19303|Walloon Coal Measures|41906|5|Briefly described|Table 2 P15|||||||||
19303|Walloon Coal Measures|41992|4|Described|Fig.2 P183|||||||||
19303|Walloon Coal Measures|42007|5|Briefly described|Fig.2 P182|||||||||
19303|Walloon Coal Measures|42182|5|Briefly described|p302|||||||||
19303|Walloon Coal Measures|42187|5|Briefly described|p321|||||||||
19303|Walloon Coal Measures|42248|5|Briefly described|p397|||||||||
19303|Walloon Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
19303|Walloon Coal Measures|42336|5|Briefly described|p4|||||||||
19303|Walloon Coal Measures|42463|6|Mentioned|Fig.3 P170|||||||||
19303|Walloon Coal Measures|42493|5|Briefly described|Fig. 1 P18|||||||||
19303|Walloon Coal Measures|42525|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|42634|6|Mentioned|p24|||||||||
19303|Walloon Coal Measures|42648|5|Briefly described|p42|||||||||
19303|Walloon Coal Measures|42719|5|Briefly described|p15|||||||||
19303|Walloon Coal Measures|42869|5|Briefly described|Table 1, P33|||||||||
19303|Walloon Coal Measures|42894|5|Briefly described|Fig.1 P20|||||||||
19303|Walloon Coal Measures|42911|5|Briefly described|p13|||||||||
19303|Walloon Coal Measures|42951|5|Briefly described|Fig.11|||||||||
19303|Walloon Coal Measures|42998|5|Briefly described|p58|||||||||
19303|Walloon Coal Measures|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
19303|Walloon Coal Measures|43001|6|Mentioned|Fig.3,p120|||||||||
19303|Walloon Coal Measures|43002|5|Briefly described|Fig.2,p135|||||||||
19303|Walloon Coal Measures|43076|5|Briefly described|p9|||||||||
19303|Walloon Coal Measures|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
19303|Walloon Coal Measures|43344|14|Not recorded|p13,14|Jurassic|Late Triassic|Part of Bundamba Group||||||
19303|Walloon Coal Measures|43383|14|Not recorded|p24,25,28|||||||||
19303|Walloon Coal Measures|43384|14|Not recorded|Map Legend||Jurassic|||||||
19303|Walloon Coal Measures|43404|14|Not recorded|Table p11||Jurassic|||||||
19303|Walloon Coal Measures|43423|4|Described|p221,222,224-5|||||||||
19303|Walloon Coal Measures|43436|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
19303|Walloon Coal Measures|43453|14|Not recorded|Map Legend|Cretaceous|Triassic|(Provisional Edition)||||||
19303|Walloon Coal Measures|43454|14|Not recorded|Map Legend|Cretaceous|Triassic|||||||
19303|Walloon Coal Measures|43459|14|Not recorded|p316|||||||||
19303|Walloon Coal Measures|43463|14|Not recorded|p8,9;map|||Spicer's Peak area,SE Qld||||||
19303|Walloon Coal Measures|43468|14|Not recorded|Map Legend||Jurassic|Provisional Edition||||||
19303|Walloon Coal Measures|43582|6|Mentioned|Fig.5,p16,28||Middle Jurassic|||||||
19303|Walloon Coal Measures|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
19303|Walloon Coal Measures|43736|6|Mentioned|p3|||||||||
19303|Walloon Coal Measures|43881|2|Defined|p6-7,11-14,37-44,55,||Jurassic|In QLD on p80,87,135. In NSW on p71-4,85-87,91-7,106-108,164.||||||
19303|Walloon Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
19303|Walloon Coal Measures|43884|14|Not recorded|p2,4||Jurassic|||||||
19303|Walloon Coal Measures|43895|14|Not recorded|p116|||||||||
19303|Walloon Coal Measures|43907|14|Not recorded|p11-13||Early Jurassic|||||||
19303|Walloon Coal Measures|43908|14|Not recorded|p1,6,26|||||||||
19303|Walloon Coal Measures|43910|14|Not recorded|p4,5,7,11,19|||||||||
19303|Walloon Coal Measures|43911|14|Not recorded|p17,18|||||||||
19303|Walloon Coal Measures|43917|14|Not recorded|p28,32|||||||||
19303|Walloon Coal Measures|43918|14|Not recorded|p54,63,64|||||||||
19303|Walloon Coal Measures|43923|6|Mentioned|p18||Jurassic|||||||
19303|Walloon Coal Measures|43924|14|Not recorded|p2,15|||See Walloon Formation.||||||
19303|Walloon Coal Measures|43925|14|Not recorded|p42,45|||||||||
19303|Walloon Coal Measures|43984|14|Not recorded|p130,131,139,140|||||||||
19303|Walloon Coal Measures|43991|4|Described|p48||Jurassic|Upper Marburg Formation.||||||
19303|Walloon Coal Measures|43993|14|Not recorded|p93-95,97-100,102||Jurassic|Ref. to Dunstan 1915.||||||
19303|Walloon Coal Measures|43995|14|Not recorded|Tb.p9&10,11-61,Map,||Early Cretaceous|Figs.3,4,9,11,15||||||
19303|Walloon Coal Measures|44021|14|Not recorded|p233 Fig.1|||Equivalent to Birkhead Formation in Eromanga Basin.||||||
19303|Walloon Coal Measures|44026|14|Not recorded|p123,124||Jurassic|||||||
19303|Walloon Coal Measures|44028|14|Not recorded|Fi.2,5,7,p509,511-14||Jurassic|Correlates with Gowen Beds. See Strat Table.||||||
19303|Walloon Coal Measures|44029|14|Not recorded|p153-5,157-8,167-8|||||||||
19303|Walloon Coal Measures|44031|14|Not recorded|p2,11|Late Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|44033|14|Not recorded|Tb.1,p4|Early Cretaceous|Jurassic|A.A.O. Beryl No.1||||||
19303|Walloon Coal Measures|44068|14|Not recorded|p15,16|||||||||
19303|Walloon Coal Measures|44077|14|Not recorded|p298|||||||||
19303|Walloon Coal Measures|44084|14|Not recorded|p2,4,6,10,12,14,16,||Middle Jurassic|p18,22,26,30,32||||||
19303|Walloon Coal Measures|44088|14|Not recorded|p6,7|||||||||
19303|Walloon Coal Measures|44089|4|Described|p4|||||||||
19303|Walloon Coal Measures|44091|14|Not recorded|p57,58||Jurassic|||||||
19303|Walloon Coal Measures|44128|14|Not recorded|Tb.1,p426|||||||||
19303|Walloon Coal Measures|44164|14|Not recorded|p24|||||||||
19303|Walloon Coal Measures|44171|14|Not recorded|p194,197,198|||Replaces Birkhead Formation.||||||
19303|Walloon Coal Measures|44240|14|Not recorded|p336|||||||||
19303|Walloon Coal Measures|44241|14|Not recorded|p6||Middle Jurassic|||||||
19303|Walloon Coal Measures|44252|14|Not recorded|p397|||||||||
19303|Walloon Coal Measures|44269|4|Described|p15,map||Jurassic|||||||
19303|Walloon Coal Measures|44375|14|Not recorded|p310|||Overlain by Blythesdale Group.||||||
19303|Walloon Coal Measures|44377|14|Not recorded|p3,8|||||||||
19303|Walloon Coal Measures|44423|14|Not recorded|p20|||||||||
19303|Walloon Coal Measures|44432|14|Not recorded|p58||Middle Jurassic|Occurs within Rosewood Stage.||||||
19303|Walloon Coal Measures|44450|4|Described|p28 Table 7|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton Basin.||||||11-DEC-07
19303|Walloon Coal Measures|44510|14|Not recorded|p259,Figs.35,36|||||||||
19303|Walloon Coal Measures|44511|14|Not recorded|p713||Early Jurassic|||||||
19303|Walloon Coal Measures|44553|14|Not recorded|p301|||||||||
19303|Walloon Coal Measures|44554|2|Defined|p288-295|||Overlies Marburg Sandstone.||||||
19303|Walloon Coal Measures|44605|14|Not recorded|p40|||||||||
19303|Walloon Coal Measures|44607|14|Not recorded|p35,36|||||||||
19303|Walloon Coal Measures|44611|14|Not recorded|p20|||||||||
19303|Walloon Coal Measures|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
19303|Walloon Coal Measures|44615|14|Not recorded|p21|||Clay deposits.||||||
19303|Walloon Coal Measures|44667|14|Not recorded|p306|||||||||
19303|Walloon Coal Measures|44674|14|Not recorded|p460|||||||||
19303|Walloon Coal Measures|44698|14|Not recorded|p111|||||||||
19303|Walloon Coal Measures|44711|14|Not recorded|p26|||Soils||||||
19303|Walloon Coal Measures|44727|14|Not recorded|p303-304|||||||||
19303|Walloon Coal Measures|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
19303|Walloon Coal Measures|44734|14|Not recorded|p5,6,13,16,19|||Pine Mountain area.||||||
19303|Walloon Coal Measures|44737|14|Not recorded|p129|||Fine grained and often calcareous in Bremer Valley, south of Rosewood.||||||
19303|Walloon Coal Measures|44752|14|Not recorded|p297|||Equivalent ot Tiaro Coal Measures.||||||
19303|Walloon Coal Measures|44774|5|Briefly described|p30||Early Jurassic|Rosewood area.||||||
19303|Walloon Coal Measures|44775|14|Not recorded|Map 2||Jurassic|||||||
19303|Walloon Coal Measures|44777|14|Not recorded|p55|||Footprints of large bipedal theropod in root shale of Striped Bacon Seam.||||||
19303|Walloon Coal Measures|44780|14|Not recorded|p297|||Flora suggests correlation with Ballow Group.||||||
19303|Walloon Coal Measures|44781|14|Not recorded|p359,363|||||||||
19303|Walloon Coal Measures|44782|2|Defined|p38,40-42,Pl.1|||||||||
19303|Walloon Coal Measures|44783|14|Not recorded|p2,20,24,26-29,43,44|||||||||
19303|Walloon Coal Measures|44784|14|Not recorded|p13,map 3||Jurassic|||||||
19303|Walloon Coal Measures|44803|14|Not recorded|p164,167||Early Jurassic|Plant fossils||||||
19303|Walloon Coal Measures|44813|14|Not recorded|p77||Jurassic|||||||
19303|Walloon Coal Measures|44819|14|Not recorded|p89|||||||||
19303|Walloon Coal Measures|45110|2|Defined|p94|Middle Jurassic|Middle Jurassic|See also p10 and p24.||||||04-JUN-07
19303|Walloon Coal Measures|45150|6|Mentioned|p2|||||||||
19303|Walloon Coal Measures|46159|14|Not recorded|p.404|||||||||
19303|Walloon Coal Measures|46791|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19303|Walloon Coal Measures|46984|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|48585|4|Described|p7,9,14,Pl.1|||||||||
19303|Walloon Coal Measures|48606|14|Not recorded|p6,Pl.1,sh.1,2|||(G/55-12).||||||
19303|Walloon Coal Measures|48611|4|Described|p9,11,Fig.2|||||||||
19303|Walloon Coal Measures|48770|6|Mentioned|p109|||||||||
19303|Walloon Coal Measures|48906|14|Not recorded|Tb.2,fig.1||Middle Jurassic|||||||
19303|Walloon Coal Measures|48908|6|Mentioned|p46||Jurassic|||||||
19303|Walloon Coal Measures|48917|3|Fully described|p24|||See stratigraphic table p13. Coal and Water p47.||||||11-DEC-07
19303|Walloon Coal Measures|48919|6|Mentioned|p58|||Refers Whitehouse (1954)||||||
19303|Walloon Coal Measures|48920|6|Mentioned|Table 7|||||||||
19303|Walloon Coal Measures|48926|6|Mentioned|p15|||P15 et seq.||||||
19303|Walloon Coal Measures|48928|6|Mentioned|p13|||Jurassic||||||
19303|Walloon Coal Measures|49010|6|Mentioned|Fig.4|||Surat Basin||||||
19303|Walloon Coal Measures|49011|6|Mentioned|Fig.3|||Surat Basin||||||
19303|Walloon Coal Measures|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Overlies: Koukandowie Volcanics.  Underlies: Main Range Volcanics.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
19303|Walloon Coal Measures|50631|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, siltstone, shale, coalseams.||||||06-JUL-04
19303|Walloon Coal Measures|60079|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|Includes: Maclean Sandstone Member.  Claystone, sandstones, coal.||||||20-JUL-04
19303|Walloon Coal Measures|60281|5|Briefly described|p22, Fig. 18 App.1|Middle Jurassic|Middle Jurassic|Interbedded sandstone, siltstone, claystone, coal, ironstone nodules. Contains the Maclean Sandstone Member. Overlain by Kangaroo Creek Sst.; overlies the Koukandowie Fm. Max. thickness: 400m. Geological Province: Clarence-Moreton, Surat & Eromanga Basins||||||
19303|Walloon Coal Measures|60699|6|Mentioned|p30|||See also informal references to Walloon coals and Walloon coal.||||||
19303|Walloon Coal Measures|60700|5|Briefly described|p37, p39|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|60993|3|Fully described|p31, p6 Fig. 2|Bathonian|Aalenian|Supersedes Walloon Beds. Conformably overlain by Kangaroo Creek Sst; conformably overlies the Marburg Subgp. Max. thickness: ~60m. Geol. Prov: Clarence-Moreton Basin-Surat Basin. Passes laterally into Birkhead Fm. Of the Injune Creek Gp.||||||
19303|Walloon Coal Measures|60995|4|Described|p67, p51 Fig. 3|Middle Jurassic|Middle Jurassic|Sandstone, siltstone, grey claystone, coal; ironstone nodules. Conformably overlies the Bundamba Gp; overlain by Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Clarence-Moreton and Surat Basins.||||||
19303|Walloon Coal Measures|60996|5|Briefly described|p125|||Characteristically contains volcaniclastic detritus. Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|60997|5|Briefly described|p138, p142 Fig. 4|Kimmeridgian|Bathonian|Characterised by sandstone rich in volcanic rock fragments and feldspar. Overlain by Kangaroo Creek Sst; conformably overlies Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|60998|6|Mentioned|p146 Fig. 2|||||||||
19303|Walloon Coal Measures|60999|5|Briefly described|p168, p175|Middle Jurassic||Overlain by Kangaroo Creek Sandstone and Grafton Formation. Geological Province: Clarence-Moreton and Surat Basins. See also p172 Fig. 6.||||||
19303|Walloon Coal Measures|61000|5|Briefly described|p181, p182|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton and Surat Basins. See also p186.||||||
19303|Walloon Coal Measures|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61002|5|Briefly described|p198 Fig 2|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61004|5|Briefly described|p230|Jurassic|Jurassic|Oil mature unit in the western and central parts of NSW, containing high vitrinite and low liptinite contents.  Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61005|5|Briefly described|p239|||Geological Province: Clarence-Moreton Basin.  See also p255 Figs. 23, 24 and 25.||||||
19303|Walloon Coal Measures|61006|5|Briefly described|p277, p289|Jurassic|Jurassic|Mudstone, labile sandstone, coal; have significant potential to generate oil. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
19303|Walloon Coal Measures|61310|4|Described|p21, p11 Fig. C2|Middle Jurassic|Middle Jurassic|Grey claystone, commonly carbonaceous or with banded coal horizons and fine- to medium-grained grey lithic sst. Overlie Marburg Subgroup units; overlain by Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Clarence-Moreton, Surat and Eromanga Basins.||||||
19303|Walloon Coal Measures|61313|6|Mentioned|p99|||Time equivalent of upper parts of Purlawaugh Formation.||||||
19303|Walloon Coal Measures|61377|5|Briefly described|p151, p142|Middle Jurassic|Middle Jurassic|Coal measure sequence of coal, tight sandstone, sltst+ shale with good oil source characteristics; excellent seal for underlying reservoirs in Hutton Fm. Conformable below Pilliga Sst. Geol.Prov: Surat Basin. See also p148 Tb. SU1, p149 Fig. SU8.||||||07-FEB-11
19303|Walloon Coal Measures|61611|5|Briefly described|p264, p265 Fig. 3|Early Jurassic|Late Triassic|Lateral equivalent to Tiaro Coal Measures. Geological Province: Surat Basin.||||||13-MAR-09
19303|Walloon Coal Measures|61617|6|Mentioned|p346 Tb. 3|||Net coal thickness: 10-25m. Geological Province: Surat Basin.||||||11-FEB-09
19303|Walloon Coal Measures|61775|6|Mentioned|p182 Fig. 1||Mesozoic|||||||
19303|Walloon Coal Measures|63218|6|Mentioned|p211.|||Reid's (1921) name for the Walloon Beds of Cameron (1907). Subsequently upgraded to Walloon Subgroup by Jones and Patrick (1981).||||||
19303|Walloon Coal Measures|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|63729|5|Briefly described|Map legend|Jurassic|Jurassic|Overlie the Marburg Subgroup; Interfinger with Kumbarilla beds. Fine- to medium-grained feldspathic sandstone and coarse-grained quartzose sandstone.||||||11-DEC-07
19303|Walloon Coal Measures|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Shale, siltstone, lithic-labile sandstone, coal, minor quartz sandstone.||||||12-DEC-07
19303|Walloon Coal Measures|63748|4|Described|p21, p23|Middle Jurassic|Middle Jurassic|Conformable on Marburg Subgroup (Bundamba Group). Unconformable below main Range Volcanics. Geol.prov:Clarence-Moreton Basin. Flat-lying sequence of lithic and feldspathic labile sandstone interbedded with siltstone, mudstone, carbonaceous shale and coal.||||||07-FEB-11
19303|Walloon Coal Measures|63979|5|Briefly described|p36, p38|||Overlies Springbok Sandstone. Geological Province: Surat and Moreton Basins.||||||07-FEB-11
19303|Walloon Coal Measures|64197|6|Mentioned|p630 Fig.7|Jurassic|Jurassic|Surat Basin.||||Underlies Springbok Sandstone; overlies Eurombah Formation.||
19303|Walloon Coal Measures|64232|6|Mentioned|p12|||Geological Province: Polda Basin.||||||24-JUL-08
19303|Walloon Coal Measures|64289|5|Briefly described|p6 Fig. 2, p11, p14|Middle Jurassic|Middle Jurassic|Geological province: Clarence-Moreton and Surat Basins.||||||07-FEB-11
19303|Walloon Coal Measures|64665|5|Briefly described|p53 Fig.2, p60, p61.|Middle Jurassic|Middle Jurassic|Surat and Clarence-Moreton Basins. It appears that Walloon Subgroup is used as an alternative name in the Surat Basin. Abundant stone and dirt bands produce high ash raw coal (30 - 40 %);  perhydrous and very hard; high volatile bituminous rank; feedstock for mine-mouth power plants but can be washed down to 12 - 17% export product.||Basal unit in Injune Creek Group.||Overlies Hutton Sandstone (Surat Basin) and Bundamba Group (Clarence-Moreton Basin).||
19303|Walloon Coal Measures|64856|3|Fully described|p79, p85-92, p102|Callovian|Bathonian|Reid (1921); formerly Walloon beds of Cameron (1907). Type section was designated as the interval 7-235m in drillhole N.S.84 by Cameron (1970). Surat Basin. Raised to Subgroup rank by Jones and Patrick in 1979. Argillaceous sandstone, siltstone, mudstone and coal. Conformably overlies Hutton Sandstone and laterally continuous with the Birkhead Formation. Up to 507m thick. Age from palynofloral units APJ42, 43, 5.|| ||||29-NOV-17
19303|Walloon Coal Measures|64857|5|Briefly described|p132-133, p113 Fig.3|||Lithic labile sandstones and coals. Relationship with underlying unit not clear: Figures show it overlying the Hutton Sandstone while text states it overlies Eurombah Formation. Surat Basin.||||||
19303|Walloon Coal Measures|64858|6|Mentioned|p180, p181 Tb.1, p187, p187 Fig.14|||Surat Basin.||||||30-NOV-09
19303|Walloon Coal Measures|64859|6|Mentioned|p195|||||||||
19303|Walloon Coal Measures|65096|5|Briefly described|p367-368, 371-374, 378, 379 Fig.7, 380|Middle Jurassic|Middle Jurassic|Eastern Surat Basin. Jones and Patrick (1981) accorded the Walloon Coal Measures sub-group status, but this was rejected by Green et al (1997). This study follows Jones and Patrick's usage. ~ 420-440 m thick in the eastern Surat Basin. Possibly exceeding 800 m in NSW.  A series of meander and back swamp deposits.|||Includes (from base) Eurombah Formation, Taroom Coal Measures,Tangalooma Sandstone, Juandah Coal Measures.|Equivalent of the Mulgildie Coal Measures, and the lower beds of the Injune Creek Group and the Birkhead Formation. Overlain by the Springbok Sandstone.|Includes high volatile bituminous coals with a high proportion of vitrinite.|
19303|Walloon Coal Measures|65112|5|Briefly described|p323, 327, 328; Fig 11 p324, fig 15 p327|Jurassic|Jurassic||166-158 Ma.|||Underlies the Springbok Sandstone; overlies the Hutton Sandstone.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|15-JAN-15
19303|Walloon Coal Measures|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Middle Jurassic|Underlies the Springbok Sandstone, overlies the Hutton Sandstone. Shown as Walloon CM.||||||
19303|Walloon Coal Measures|65114|5|Briefly described|p385 Fig.3|Late Jurassic|Middle Jurassic|Written as Walloon CM||||||
19303|Walloon Coal Measures|65116|5|Briefly described|p455, Fig 2 p437|Late Jurassic|Middle Jurassic|Underlies the Springbok Sandstone, overlies the Hutton Sandstone, Surat Basin. Interbedded lithic sandstone, siltstone, mudstone and coal.||||||
19303|Walloon Coal Measures|65117|4|Described|p461, 462-3, 469-72, Fig 4 p465, 466|Callovian|Bathonian|Surat Basin. Overlies and interfingers with Eurombah Formation. Overlain by Springbok Sandstone. Sandstone, siltstone, mudstone and rare to abundant coal seams. Thickness up to 650m. Base of unit youngs to west. Coal seam gas source.||||||
19303|Walloon Coal Measures|65119|6|Mentioned|p526, Fig 6 p512, Fig 13-14|Late Jurassic|Middle Jurassic|Of Injune Creek Group. Coal.||||||
19303|Walloon Coal Measures|65388|5|Briefly described|p215, 216|Callovian|Bathonian|Of Injune Creek Group. Correlated with Mulgildie Coal Measures on stratigraphic and lithological grounds. Conformably (transitionally) overlies Hutton Sandstone. Age: late Middle Jurassic (Bathonian to Callovian), based on palynofloras attributed to units APJ42, APJ43 and APJ5 (Price, 1997).||||||
19303|Walloon Coal Measures|65489|6|Mentioned|p24|||Volcanic-arc-derived sediments.||||||
19303|Walloon Coal Measures|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Hutton Sandstone and Eurombah Formation. Is overlain by Injune Creek Group, Kumbarilla beds and Pilliga Sandstone.||
19303|Walloon Coal Measures|66915|5|Briefly described|p6 Fig.3, p9|Middle Jurassic|Middle Jurassic|Surat Basin.||Injune Creek Group.||||
19303|Walloon Coal Measures|67365|5|Briefly described|p81, p85, p86. |Middle Jurassic|Middle Jurassic|Surat Basin. Coal seam gas extraction was applied to this field from 2000. High volatile, perhydrous, sub-bituminous and non-coking coals with moderate gas contents (5-10 m3 per tonne) and generally high permeabilities.|||Includes Juandah and Taroom Coal Members.|||
19303|Walloon Coal Measures|67402|6|Mentioned|p161, p188|Bajocian|Aalenian|||Walloon Subgroup||||
19303|Walloon Coal Measures|68003|5|Briefly described|p55 Fig.3-m, p57 Fig.3-n, pp63-64, p127.|Middle Jurassic|Middle Jurassic|Northern Brigalow Belt South Bioregion. Stratigraphic equivalent of upper part of Purlawaugh Formation. Deposited in meandering streams and swamps. Outcrops very poorly. Coal seams are more abundant towards the top. Subsurface, thickens northward to 180 m.||||Conformably overlies Hutton Sandstone. Is overlain conformably by Pilliga Sandstone and Springbok Sandstone.|Grey, lithic, labile sandstone, calcareous in places; granular to pebble conglomerate; grey siltstone; medium to dark grey and chocolate-brown mudstone; dull brown to shiny black coal.|
19303|Walloon Coal Measures|68004|5|Briefly described|p139, p163-164.|Jurassic|Jurassic|Kaolin prospectivity is discussed. Contains minor coal intervals with limited prospects. However, this unit is largely unexplored and there are several coal mines within this unit in Queensland. Forms a seal for Hutton Sandstone.||||||
19303|Walloon Coal Measures|68006|5|Briefly described|pp91-92.|Jurassic|Jurassic|A 3 m coal interval was intersected in water bores NE of Warialda, suggesting limited potential. However, the area is largely unexplored, and there are several coal mines within this unit in Queensland.||||Is overlain by Pilliga Sandstone.||
19303|Walloon Coal Measures|68008|5|Briefly described|p241-243, p246|Middle Jurassic|Middle Jurassic|Moreton Basin. Coal seams typically are lenticular with marked thickness variations and seam splitting.||||Correlated with Mulgildie Coal Measures.||
19303|Walloon Coal Measures|68117|5|Briefly described|p345, p347|||Reid (1921); previously the Walloon Beds of Cameron (1907). A type area near Walloon township was specified by Whitehouse (1955). Upgraded to Walloon Subgroup by Jones and Patrick (1981).||||Overlay Eurombah Formation. Overlain by Springbok Sandstone.||
19303|Walloon Coal Measures|68135|5|Briefly described|p49-50, p52-55, p57-58, p61-64|Callovian|Bajocian|Clarence-Moreton and Surat Basins. Important source of thermal coal and (in the Surat Basin) coal seam gas. Includes plant macrofossils, vertebrate fossils and tracks (dinosaur footprints dated c.168-161 Ma). Plant fossils listed; fish fossils illustrated.||||Overlies Hutton Sandstone, Koukandowie Formation. Is unconformably overlain by Kangaroo Creek and Springbok Sandstones.|Interbedded coal, mudstone and sandstone; volcanic ash beds.|15-SEP-17
19303|Walloon Coal Measures|68139|5|Briefly described|p23|Middle Jurassic|Middle Jurassic|Continuous across the Surat and Clarence-Moreton Basin (QLD and northern NSW). A prolific, low-rank coal seam gas resource. Fluvio-lacustrine environment.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Springbok Sandstone.|Very fine- to medium-grained litharenite, shale, siltstone, mudstone, minor limestone, ironstone (siderite) and coal. Includes volcanic debris and widespread ash-fall tuffs.|
19303|Walloon Coal Measures|68327|5|Briefly described|Map legend.|Jurassic|Jurassic||||||Shale, siltstone, sandstone, coal seams.|
19303|Walloon Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Clarence-Moreton and Surat Basins. This unit, as well as the Injune Creek Group and the Mulgildie Coal Measures, are all mapped under the symbol, Ji.||||||
19303|Walloon Coal Measures|68576|5|Briefly described|Q_4: p3|Middle Jurassic|Middle Jurassic|Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain unconformably by Springbok Sandstone.||
19303|Walloon Coal Measures|68679|5|Briefly described|p312-313, p455, p472|Jurassic|Jurassic|Northern New England Orogen.||||||
19303|Walloon Coal Measures|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
19303|Walloon Coal Measures|69297|4|Described|p370, p386, p486|Upper Jurassic|Middle Jurassic|Clarence-Moreton Basin. Oil prone source rocks are present. Maximum thickness of approximately 600m. Deposited as sandy channel fill or overbank/floodplain deposits as part of a meandering fluvial system. See also p487 fig 5.38, p488, p489.|||Includes the Maclean Sandstone Member.|Overlies the Bundamba Group. Overlain by the Kangaroo Creek Sandstone.|Interbedded sandstone, siltstone, claystone, coal and ironstone nodules.|
19303|Walloon Coal Measures|69582|5|Briefly described|p35, p38|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies the Hutton Sandstone. Unconformably overlain by the Springbok Sandstone.|Sandstones, siltstones, mudstones and coal seams.|
19303|Walloon Coal Measures|69594|4|Described|p517, p519, p524, p536-537, p539|Middle Jurassic|Middle Jurassic|See also p544-547, p549, p573. Surat, Clarence-Moreton and Nambour Basins. First defined in the Clarence-Moreton Basin (Cameron, 1907; others listed). Swarbrick (1973) divided the Walloon Coal Measures (WCM) into six units in the NE Surat Basin; Jones and Patrick (1981) raise WCM to Subgroup status to include the Taroom Coal Measures, Tangalooma Sandstone and Juandah Coal Measures. Green et al. (1997), unable to distinguish the Eurombah Formation, included it within the WCM. Scott et al. (2004) succeeded in the NE Surat Basin, and so they are here regarded as members of the WCM [without the Rank term Member attached]. The WCM is not regarded here as warranting Subgroup status. Tectonic significance of volcanic ash beds discussed. Highly sinuous fluvial deposits in the lower part; coal swamps in the upper. Bathonian-Callovian palynomorphs. An important thermal coal, CSG and LNG resource (described). Minor source of bentonite. RELATED UNITS (continued): Is laterally equivalent to the Birkhead Formation and Tiaro Coal Measures.||Injune Creek Group.||Overlies Hutton Sandstone (conformably/transitionally) and Koukandowie Formation. Is overlain unconformably by Springbok Sandstone and Kangaroo Creek Sandstone (locally disconformably/conformably).|Labile sandstones, siltstone, mudstone and coal in the upper half to two-thirds of the formation, with lesser calcareous sandstone, impure limestone and ironstone. Coal decreases markedly to the WE. Includes silicic tuffs.|
19303|Walloon Coal Measures|69599|6|Mentioned|p595|||||||Is overlain unconformably by the Beaudesert beds.||
19303|Walloon Coal Measures|69633|5|Briefly described|p3|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies Hutton Sandstone.||
19303|Walloon Coal Measures|69681|6|Mentioned|p74 Fig.3|Middle Jurassic|Middle Jurassic|||Unit in Injune Creek Group.||||
19303|Walloon Coal Measures|69682|5|Briefly described|p95 Fig.3|Middle Jurassic|Middle Jurassic|Name replaced by Walloon Subgroup.||||||
19303|Walloon Coal Measures|69790|5|Briefly described|p1063 Fig.2, p1065-1066|||Cameron (1970). Jones and Patrick (1981) raised this unit to Walloon Subgroup, in the NE Surat Basin. Northern Clarence-Moreton Basin area.||||Overlies Eurombah Formation. Is overlain by Springbok Sandstone.||
19303|Walloon Coal Measures|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
19303|Walloon Coal Measures|69946|6|Mentioned|p13-14, p75|||W Surat Basin.||||||
19303|Walloon Coal Measures|69947|5|Briefly described|p23 Fig.7.12|||Surat Basin. Volcanic-arc-derived sediments.||||Overlies Hutton Sandstone.|Lithic arenites, coal.|
19303|Walloon Coal Measures|70036|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Surat Basin. Included in a mapped unit of fluvial and lacustrine sequences: lithic to quartzose sandstone, siltstone, mudstone, claystone and coal.||||||
19303|Walloon Coal Measures|70374|4|Described|p807-814|Oxfordian|Aalenian|Surat and Clarence-Moreton Basins. Type section in Clarence Moreton Basin is difficult to relate to the occurences in the Surat Basin. Originally used by Bryan (1944). 350-450 m thick. Age determined by biostratigraphy in past, as in the 174.1 - 163.5 Ma range (Aalenian to Callovian). Maximum age in Clarence Moreton Basin (Aalenian) may be older than in Surat Basin, where age is now constrained by dating of tuffs in the Taroom Coal Measures and the Juandah Coal Measures.|~162 - 158 Ma CA-TIMS.|Lower part of Injune Creek Group.|Includes Taroom Coal Measures, Tangalooma Sandstone, Maclean Sandstone Member, Juandah Coal Measures.|Conformably overlies Hutton Sandstone or Eurombah Formation. Underlies Springbok Sandstone unconformably. Shown as lateral equivalent of Birkhad Formation.|Include tuff layers.|
19303|Walloon Coal Measures|70628|6|Mentioned|p952|Jurassic|Jurassic|Informally renamed Walloon Subgroup.||||||
19303|Walloon Coal Measures|70725|5|Briefly described|p12-14, 18-19, 24, 26|Late Jurassic|Late Jurassic|Surat Basin. Up to c.450m thick. Oxfordian. Diverse contributing plant taxa listed and discussed.|162-158 Ma.|Walloon Subgroup.|Taroom, Lower Juandah, Upper Juandah, Coal Measures; Tangalooma, Wambo Sandstones||Sub-bituminous rank coals.|
19303|Walloon Coal Measures|70820|6|Mentioned|p36-37|||Contains considerable coal seam gas reserves and is a target for potential extraction in the Richmond River catchment.||||||
19303|Walloon Coal Measures|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone or Koukandowie Formation (Marburg Subgroup, Bundamba Group). Is overlain by Springbok, Pilliga or Mooga Sandstones, or Kumbarilla beds.||
19303|Walloon Coal Measures|71342|5|Briefly described|Ch5 p14, Ch5 p74|||Surat Basin. See also the Birkhead Formation. Power and Devine (1968) recommended that this unit supersede the Birkhead Formation.||||||
19303|Walloon Coal Measures|71601|6|Mentioned|p120 , p121|Bathonian|Bajocian|SE Qld. Includes a possible stegosaur track.||||||
19303|Walloon Coal Measures|71805|6|Mentioned|p77, p86|||Surat Basin.||||||15-MAY-19
19303|Walloon Coal Measures|71863|6|Mentioned|p2|Mesozoic|Mesozoic|||||||
19303|Walloon Coal Measures|72297|5|Briefly described|p698-700, p739, p745-746, p750-751|Middle Jurassic|Middle Jurassic|Clarence-Moreton, Surat and Mulgildie Basins. Perhydrous cannel coals; characteristics and use in thermal power stations described. Produces commercial CSG and is a target of further exploration. Potential hydrocarbon source rock, but unlikely to have reached thermal maturity.||||Overlies Eurombah Formation ?conformably. Is overlain unconformably by Springbok Sandstone. Correlative of Mulgildie Coal Measures.|Coal seams in thick, banded intervals, separated by lenticular beds of carbonaceous shale, mudstone, siltstone and sandstone of varying thickness.|
19303|Walloon Coal Measures|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW).||Injune Creek Group.||Overlies Eurombah FZ and Hutton Sandstone. Is overlain by Springbok and Pilliga Sandstones and Kumbarilla beds.||
19303|Walloon Coal Measures|72478|6|Mentioned|p62 (digital)|||Surat Basin. Mid-Jurassic. Contains significant gas reserves. Lithology compared to Boorthanna Formation.|||||Said to contain sub-bituminous coal deposits.|
19303|Walloon Coal Measures|72921|4|Described|p13, p15 Fig.2, p16-17, p24, p47.|Middle Jurassic|Middle Jurassic|Includes a marine influence. Mostly swampy, fresh water. Interpreted as correlative across the Clarence-Moreton, Surat and Eromanga Basins. Shown as located within the Clarence-Moreton Basin, and the Surat Basin in Queensland. See also Walloon Subgroup p8, 13. See also p49-51, p54.||||Overlies Durabilla and Eurombah Formations, Koukandowie Formation and is shown as unconformably underlying Springbok Sandstone, Kangaroo Creek Sandstone.|Includes crossbedded sandstone, shales and siltstone. Also includes polymictic conglomerate and crossbedded sandstones.|
19303|Walloon Coal Measures|73113|5|Briefly described|p. 2, 10, 13-14, 16, 19, 22-24, 27-29...|||Surat Basin. 300 m thick in some places. Percentage of coal varies from <1 to ~20% (mean 8.5%). Groundwater model divides unit into lower, 3 middle, upper, and non-productive zones (layers). Interbedded aquitard. Incised by up to 120 m. Top contact zone forms the ""Condamine Alluvium transition zone"" ca 1-15 m thick. Non-productive part is relatively thin; <10 m. More locations: p. 31, 36-38, 41, 45, 49, 51-52, 57-58, 60-62, 66-71, 78, 80-82, 86, 89, 91, 94, 96-108, 116-117, 119, 123-124, 126-130, 132, 134, 136-138, 143, 145-150, 152, 154, 158-164, 166-169, 172-175, 177, 179-180, 191-194, 196, 199-200, 208.||||Underlain by Durabilla Formation. Overlain by Springbok Sandstone and unconformably by Condamine Alluvium.|Discontinuous permeable coal seams interbedded with low-permeability material consisting of siltstones, mudstones and fine-grained sandstones. Includes a top weathered/clay interval.|
19303|Walloon Coal Measures|73147|5|Briefly described|p127, 135-136, 140, 144|Late Jurassic|Middle Jurassic|Surat Basin. Shallow fluvial-estuarine setting with marine incursions.||||Coeval with Loth Formation.|Structureless to horizontally laminated fine-grained sandstones, siltstones and mudstones. Silicic tuff is widespread.|
19303|Walloon Coal Measures|73200|4|Described|p531-p533, p535, p539-542|Jurassic|Jurassic|Abbreviated to WCM in text. ca 159 Ma age from Wainman et al., (2015). Deposited in a fluvio-lacustrine environment with peat-forming conditions and contemporaneous volcanism during the Middle Jurassic, lithification was prior to the mid-Cretaceous (Hamilton et al., 2014). Mineral composition in upper section is predominantly kaolin, quartz and feldspar, with gypsum prevalent in carbonaceous layers.|ca 159 Ma||Macalister Seam|Angularly underlies the Condamine Alluvium, underlies the Kumbarilla Beds, Main Range Volcanics. Overlies the Marburg Sandstone.|Discontinuous thin coal seams in mudstone and siltstone with minor calcareous sandstone, limestone and ironstone matrix. Carbonaceous mudstone, thin and mostly dull coal, thin tuffs, lapilli and minor siltstone with minor weathering in upper section.|
19303|Walloon Coal Measures|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Marburg Subgroup (Bundamba Group). Is overlain by Kangaroo Creek Sandstone.||
19303|Walloon Coal Measures|73393|6|Mentioned|p19-22|Tithonian|Callovian|Surat Basin. Previously called the Walloon Series. The only pre-Cretaceous sauropod known from Australia, Rhoetosaurus brownei, was recovered from this unit (collected from the banks of a gully feeding the Eurombah Creek on Taloona Station, SE QLD). Detrital zircons collected alongside the fossil specimen yielded a maximum depositional age of 162.6 +/- 1.1 Ma; consistent with the unit's age range of ca 165-151 Ma from Wainman et al. (2015, 2018a, 2018b). This indicates the fossil was probably from the lower portion of the unit.|ca 165-151 Ma|Injune Creek Group||Underlain by Eurombah Formation. Overlain by Springbok Sandstone. Equivalent to Birkhead Formation.||
19303|Walloon Coal Measures|73570|6|Mentioned|p912 Fig.2, p920|||||||||
19323|Wallumbilla Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Dark purplish grey to white, fine to medium lithic sandstone, feldspathic sandstone.||||||
19323|Wallumbilla Formation|12597|4|Described|p492 Tb.1, p497, p498, p499-500|Albian|Aptian|Eromanga Basin. Division into the two Members is not possible in the NW, where the sequence is more uniform.|||Includes Doncaster and Coreena Members.||Marine, largely argillaceous sequence with common mollusc, gastropod, scaphopod and belemnites fossils.|
19323|Wallumbilla Formation|13497|5|Briefly described|p115 fig 6.33, p138 fig 8.17|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p144 fig 9.2, p145, p146, p148-p151.||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Doncaster and Coreena Members|||
19323|Wallumbilla Formation|22464|5|Briefly described|p9||Early Cretaceous|Eromanga Basin. Overlain by Toolebuc Formation.||||||18-DEC-06
19323|Wallumbilla Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
19323|Wallumbilla Formation|22747|6|Mentioned|p15||Mesozoic|||||||
19323|Wallumbilla Formation|22757|6|Mentioned|Table6,p11||Early Cretaceous|In the Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|22857|4|Described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of the Rolling Downs Group. Sequence of mudstone and siltstone. Contains the Coreena Member. Max. thickness: 600m. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p314-5, p544 App.1 Tb.A1.12.||||||
19323|Wallumbilla Formation|22865|4|Described|p314,Table22.1p296-7|Albian|Aptian|||||||
19323|Wallumbilla Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Toolebuc Formation, underlying unit is Cadna-owie Formation||||||
19323|Wallumbilla Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23031|5|Briefly described|31|||||||||
19323|Wallumbilla Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19323|Wallumbilla Formation|23065|5|Briefly described|18|||Geological  province: Carpentaria Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23071|6|Mentioned|p761|||||||||
19323|Wallumbilla Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||18-DEC-06
19323|Wallumbilla Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The unit is laterally equivalent to the Bulldog Shale and it is limited to the northern part of STRZELECKI.  Age Aptian-Albian.||||||
19323|Wallumbilla Formation|23183|6|Mentioned|p222||Aptian|||||||
19323|Wallumbilla Formation|23220|5|Briefly described|p16||Mesozoic|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23224|5|Briefly described|p3|||Hosts the Doncaster Member which hosts the Opal Deposits. Of Rolling Downs Group. In the Great Australian Basin.||||||01-FEB-07
19323|Wallumbilla Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: early Cretaceous. Conformably overlies Coffin Hill Member. Geological Province: Georgetown Region.||||||08-JUL-15
19323|Wallumbilla Formation|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Bulldog Shale. of Eromanga Basin.||||||
19323|Wallumbilla Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|23425|4|Described|Table 9.7 p394|Aptian|Aptian|+ Plate 9.2 + p378. Of Rolling Downs Group. Conformably overlain by Toolebuc Formation; underlain by Gilbert River Formation. Geological Province Carpentaria Basin. Max. thickness 500 m.||||||18-DEC-06
19323|Wallumbilla Formation|23430|5|Briefly described|p455|||Eromanga Basin Province.||||||
19323|Wallumbilla Formation|23496|5|Briefly described|Table 4, p59|Albian|Aptian|of Rolling Downs Group. Previously Blackdown Formation (Laing and Power 1959), then Wilgunya Subgroup (Grimes & Whittaker 1977) then of Smart and Others 1972/1980.||||||01-FEB-07
19323|Wallumbilla Formation|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|In the Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23510|5|Briefly described|Map Legend||Early Cretaceous|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|23713|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Wilunga Sub-Group.||||||
19323|Wallumbilla Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Contains the Coreena and Doncaster Members.  Geological Province: Great Australian Superbasin.||||||
19323|Wallumbilla Formation|23911|5|Briefly described|p90 Fig. 4|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
19323|Wallumbilla Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Includes the Coreena and Doncaster Members. Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|23986|5|Briefly described|p71|||||||||
19323|Wallumbilla Formation|24048|5|Briefly described|p76|||||||||
19323|Wallumbilla Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 310m.||||||
19323|Wallumbilla Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Supersedes Balckdown Formation.  Of Rolling Downs Group. Maximum thickness: 200m.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|24085|5|Briefly described|Not recorded|Albian|Aptian|Contains Doncaster Member. Geological Province: Eromanga Basin||||||16-MAR-05
19323|Wallumbilla Formation|24092|5|Briefly described|p5|Cretaceous|Jurassic|Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Aptian|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup?  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Toolebuc Formation. Geological Province: Eromanga Basin||||||
19323|Wallumbilla Formation|29387|6|Mentioned|Table 5|||||||||
19323|Wallumbilla Formation|29393|6|Mentioned|Table 4|||Cretaceous.||||||
19323|Wallumbilla Formation|29591|6|Mentioned|p71|||||||||
19323|Wallumbilla Formation|29651|6|Mentioned|p25|||||||||
19323|Wallumbilla Formation|29721|6|Mentioned|Table 246|||||||||
19323|Wallumbilla Formation|30019|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|30020|4|Described|p29|||||||||
19323|Wallumbilla Formation|30021|6|Mentioned|p89|||||||||
19323|Wallumbilla Formation|30022|6|Mentioned|p32|||||||||
19323|Wallumbilla Formation|30024|6|Mentioned|p331|||||||||
19323|Wallumbilla Formation|30042|4|Described|p4|||? glauconite.||||||
19323|Wallumbilla Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30102|6|Mentioned|Table 4|Cretaceous|Jurassic|See also P17.||||||
19323|Wallumbilla Formation|30103|5|Briefly described|p9|||Table 3 on p9.||||||18-DEC-06
19323|Wallumbilla Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30443|6|Mentioned|p2|||See also P4. Aptian age||||||
19323|Wallumbilla Formation|30446|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|30458|6|Mentioned|p7|||Cretaceous age||||||
19323|Wallumbilla Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19323|Wallumbilla Formation|30584|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30691|4|Described|Table 4|||Lower-Upper Cretaceous age. Of Rolling Downs Group||||||
19323|Wallumbilla Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Lower Cretaceous age||||||
19323|Wallumbilla Formation|30695|4|Described|Table 4|||Lower Cretaceous age.||||||17-SEP-08
19323|Wallumbilla Formation|30696|4|Described|Table 4|||Aptian-Albian age||||||
19323|Wallumbilla Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30700|6|Mentioned|p22|||Lower Cretaceous age. Map||||||
19323|Wallumbilla Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19323|Wallumbilla Formation|30804|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|30853|5|Briefly described|Table 3|||Aptian to Lower Albian age||||||
19323|Wallumbilla Formation|30854|4|Described|Table 4|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit in Rolling Downs Group||||||
19323|Wallumbilla Formation|30856|4|Described|Table 3|||Lower Cretaceous age.||||||
19323|Wallumbilla Formation|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|30915|6|Mentioned|Table|||Shown on stratigraphic table||||||
19323|Wallumbilla Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31116|4|Described|p43|||See also Table 2. Cretaceous||||||
19323|Wallumbilla Formation|31120|6|Mentioned|Table|||||||||
19323|Wallumbilla Formation|31121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31164|5|Briefly described|p8|||Aptian - Lower Albian, See also P10.||||||
19323|Wallumbilla Formation|31165|6|Mentioned|Table 11|||||||||
19323|Wallumbilla Formation|31168|6|Mentioned|p10|||||||||
19323|Wallumbilla Formation|31208|6|Mentioned|Fig 36|||See also Table 1||||||
19323|Wallumbilla Formation|31209|4|Described|p159|||||||||
19323|Wallumbilla Formation|31376|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, glauconitic sandstone.||||||02-DEC-04
19323|Wallumbilla Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
19323|Wallumbilla Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31433|5|Briefly described|p6|||L.Cretaceous||||||
19323|Wallumbilla Formation|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous.||||||17-SEP-08
19323|Wallumbilla Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31832|6|Mentioned|Table 6|||||||||
19323|Wallumbilla Formation|32136|6|Mentioned|p3|||Continuously cored composite section||||||
19323|Wallumbilla Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32275|4|Described|p8|||||||||
19323|Wallumbilla Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32313|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|32314|6|Mentioned|Fig. 4|||||||||
19323|Wallumbilla Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
19323|Wallumbilla Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
19323|Wallumbilla Formation|32490|6|Mentioned|p9|||Crops out W of Buchanan sheet||||||
19323|Wallumbilla Formation|32553|4|Described|p38|||||||||
19323|Wallumbilla Formation|32705|6|Mentioned|p188|||||||||
19323|Wallumbilla Formation|32796|6|Mentioned|p302|||||||||
19323|Wallumbilla Formation|32797|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33016|6|Mentioned|p1|||On table||||||
19323|Wallumbilla Formation|33017|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, siltstone,minor sandstone.||||||07-JUL-04
19323|Wallumbilla Formation|33069|4|Described|p7|||L.Cret.||||||
19323|Wallumbilla Formation|33070|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33071|4|Described|p2|||L.Cret.||||||
19323|Wallumbilla Formation|33072|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33075|6|Mentioned|p445|||||||||
19323|Wallumbilla Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
19323|Wallumbilla Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33088|4|Described|Table 3|||||||||
19323|Wallumbilla Formation|33089|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33090|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
19323|Wallumbilla Formation|33092|5|Briefly described|p6|||Strat. table||||||
19323|Wallumbilla Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33150|4|Described|p9|||L.Cret.||||||
19323|Wallumbilla Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33165|6|Mentioned|Chart|||Correlatin chart only||||||
19323|Wallumbilla Formation|33175|6|Mentioned|p280|||||||||
19323|Wallumbilla Formation|33176|5|Briefly described|p172|||||||||
19323|Wallumbilla Formation|33177|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|33178|6|Mentioned|p11|||||||||
19323|Wallumbilla Formation|33179|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33182|6|Mentioned|p190|||||||||
19323|Wallumbilla Formation|33183|6|Mentioned|p233|||||||||
19323|Wallumbilla Formation|33368|6|Mentioned|p24|||Geol.Map.||||||
19323|Wallumbilla Formation|33372|4|Described|p17|||See also p20. From QDM Aramac 1.||||||18-DEC-06
19323|Wallumbilla Formation|33414|6|Mentioned|p212-214,Tb.||Aptian|Part of Wilgunya Sub-Group..||||||
19323|Wallumbilla Formation|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
19323|Wallumbilla Formation|33449|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33561|6|Mentioned|p102|||||||||
19323|Wallumbilla Formation|33638|5|Briefly described|Table 1|||||||||
19323|Wallumbilla Formation|33639|5|Briefly described|p11|||L.Cret.||||||
19323|Wallumbilla Formation|33640|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33642|1|Redefined|p148|Early Cretaceous|Early Cretaceous|Includes Doncaster, Jones Valley, Ranmoor and Coreena Members. Contains Roma and older part of Tambo fauna of Aptian and Albian (Lower Cret)||||||
19323|Wallumbilla Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33646|6|Mentioned|p8|||Strat. table.||||||
19323|Wallumbilla Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33648|6|Mentioned|p20|||||||||
19323|Wallumbilla Formation|33672|5|Briefly described|p44|||Lithology.||||||
19323|Wallumbilla Formation|33673|4|Described|p292|||||||||
19323|Wallumbilla Formation|33772|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33773|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33825|6|Mentioned|p10|||Correlation table||||||
19323|Wallumbilla Formation|33832|5|Briefly described|p11|||Strat. and correlation.||||||18-DEC-06
19323|Wallumbilla Formation|33900|6|Mentioned|p21|||||||||
19323|Wallumbilla Formation|33939|6|Mentioned|p412|||||||||
19323|Wallumbilla Formation|33964|4|Described|p6|||Refers Vine et al. (1967).||||||
19323|Wallumbilla Formation|34065|4|Described|p6|||L.Cret.||||||
19323|Wallumbilla Formation|34091|5|Briefly described|Table 1|||See also P4. L.Cret. Part of Rolling Downs Group.||||||
19323|Wallumbilla Formation|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34212|6|Mentioned|p2|||Cretaceous||||||
19323|Wallumbilla Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34218|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
19323|Wallumbilla Formation|34356|6|Mentioned|p13|||Lower Cretaceous.||||||
19323|Wallumbilla Formation|34485|5|Briefly described|Table 1,p10|||Lower Cretaceous||||||
19323|Wallumbilla Formation|34486|5|Briefly described|Table 1|||Lower Cretaceous. See also Table 2||||||
19323|Wallumbilla Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19323|Wallumbilla Formation|34613|4|Described|Table 4|||||||||
19323|Wallumbilla Formation|34811|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35139|4|Described|Table.2|||||||||
19323|Wallumbilla Formation|35239|6|Mentioned|p258|||||||||
19323|Wallumbilla Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
19323|Wallumbilla Formation|35560|4|Described|p290|||||||||
19323|Wallumbilla Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
19323|Wallumbilla Formation|35793|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|35811|5|Briefly described|Table 3|||||||||
19323|Wallumbilla Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
19323|Wallumbilla Formation|35936|6|Mentioned|p615|||||||||
19323|Wallumbilla Formation|35937|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|36012|3|Fully described|Table 5|||See also p18.||||||18-DEC-06
19323|Wallumbilla Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|36243|6|Mentioned|Table 6A|||||||||
19323|Wallumbilla Formation|36251|4|Described|p3|||||||||
19323|Wallumbilla Formation|36570|5|Briefly described|p50|||See also p60.||||||18-DEC-06
19323|Wallumbilla Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
19323|Wallumbilla Formation|36574|6|Mentioned|p602|||||||||
19323|Wallumbilla Formation|36580|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|36581|6|Mentioned|p464|||||||||
19323|Wallumbilla Formation|36910|6|Mentioned|p61|||||||||
19323|Wallumbilla Formation|37117|5|Briefly described|p313|||||||||
19323|Wallumbilla Formation|37451|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|37597|6|Mentioned|p77|||||||||
19323|Wallumbilla Formation|37608|3|Fully described|Table 1 p316-319|||||||||
19323|Wallumbilla Formation|37995|4|Described|p66|||||||||
19323|Wallumbilla Formation|38199|5|Briefly described|p423|||Palynology||||||
19323|Wallumbilla Formation|38218|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|38226|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|38372|6|Mentioned|p651|||||||||
19323|Wallumbilla Formation|38373|6|Mentioned|p619|||||||||
19323|Wallumbilla Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19323|Wallumbilla Formation|38779|6|Mentioned|p7|||||||||
19323|Wallumbilla Formation|38780|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|38814|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Gilbert River Formation.||||||25-AUG-04
19323|Wallumbilla Formation|39070|4|Described|p364|||||||||
19323|Wallumbilla Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,11-15 etc. Correlation||||||
19323|Wallumbilla Formation|39212|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|39216|6|Mentioned|p55|||||||||
19323|Wallumbilla Formation|39445|5|Briefly described|Table 11|||||||||
19323|Wallumbilla Formation|39478|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39627|6|Mentioned|p269|||||||||
19323|Wallumbilla Formation|39708|6|Mentioned|p478|||||||||
19323|Wallumbilla Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39846|6|Mentioned|p44|||||||||
19323|Wallumbilla Formation|39847|5|Briefly described|p38|||||||||
19323|Wallumbilla Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39942|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|39943|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|39988|6|Mentioned|p288|||||||||
19323|Wallumbilla Formation|39989|4|Described|p423|||||||||
19323|Wallumbilla Formation|40058|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|40150|6|Mentioned|p81|||||||||
19323|Wallumbilla Formation|40199|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40218|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|40245|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|40249|6|Mentioned|p38|||Mention P41||||||
19323|Wallumbilla Formation|40250|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40452|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40541|3|Fully described|p111|||||||||
19323|Wallumbilla Formation|40544|6|Mentioned|p159|||||||||
19323|Wallumbilla Formation|40623|5|Briefly described|p108|||||||||
19323|Wallumbilla Formation|40648|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|40659|6|Mentioned|p250|||||||||
19323|Wallumbilla Formation|40666|4|Described|p358|||||||||
19323|Wallumbilla Formation|40670|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|40675|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|40687|3|Fully described|p418|||||||||
19323|Wallumbilla Formation|40771|6|Mentioned|p429|||||||||
19323|Wallumbilla Formation|40801|6|Mentioned|p29|||See also P39||||||
19323|Wallumbilla Formation|40832|3|Fully described|p457|||||||||
19323|Wallumbilla Formation|40833|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|40926|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|40962|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41012|5|Briefly described|p137|||||||||
19323|Wallumbilla Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
19323|Wallumbilla Formation|41062|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|41063|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|41064|6|Mentioned|p60|||||||||
19323|Wallumbilla Formation|41084|5|Briefly described|Fig.2|||||||||
19323|Wallumbilla Formation|41086|3|Fully described|p98, Fig.3|||Mentioned p101.||||||18-DEC-06
19323|Wallumbilla Formation|41087|6|Mentioned|p123|||||||||
19323|Wallumbilla Formation|41088|6|Mentioned|p141|||||||||
19323|Wallumbilla Formation|41097|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|41099|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|41117|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|41165|5|Briefly described|p362|||||||||
19323|Wallumbilla Formation|41175|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41176|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|41177|6|Mentioned|p225|||||||||
19323|Wallumbilla Formation|41178|6|Mentioned|p242|||||||||
19323|Wallumbilla Formation|41182|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|41183|6|Mentioned|p310|||||||||
19323|Wallumbilla Formation|41184|6|Mentioned|p347|||||||||
19323|Wallumbilla Formation|41186|6|Mentioned|p197|||||||||
19323|Wallumbilla Formation|41187|6|Mentioned|p227|||||||||
19323|Wallumbilla Formation|41196|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41198|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41214|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41216|6|Mentioned|Fig.18|||||||||
19323|Wallumbilla Formation|41246|6|Mentioned|Map legend|Cretaceous||||||||
19323|Wallumbilla Formation|41266|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41286|6|Mentioned|p118|||||||||
19323|Wallumbilla Formation|41306|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|41307|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|41361|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41427|6|Mentioned|p84|||||||||
19323|Wallumbilla Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41523|3|Fully described|p278|||||||||
19323|Wallumbilla Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41568|5|Briefly described|p15|||||||||
19323|Wallumbilla Formation|41681|6|Mentioned|p11,p22|||||||||
19323|Wallumbilla Formation|41707|6|Mentioned|p164|||||||||
19323|Wallumbilla Formation|41992|4|Described|Fig.2 p183|||||||||26-APR-18
19323|Wallumbilla Formation|42007|5|Briefly described|p182|||||||||
19323|Wallumbilla Formation|42061|4|Described|p157|||See also Fig.11||||||
19323|Wallumbilla Formation|42067|5|Briefly described|p309|||See also Appendix 2||||||
19323|Wallumbilla Formation|42071|6|Mentioned|p117|||||||||
19323|Wallumbilla Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19323|Wallumbilla Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19323|Wallumbilla Formation|42369|5|Briefly described|Fig.10, P61|||||||||
19323|Wallumbilla Formation|42397|6|Mentioned|Fig.2 P3|||||||||
19323|Wallumbilla Formation|42429|5|Briefly described|Fig.3 P155|||||||||
19323|Wallumbilla Formation|42446|4|Described|p13|||||||||
19323|Wallumbilla Formation|42447|6|Mentioned|p16|||||||||
19323|Wallumbilla Formation|42474|5|Briefly described|p25|||||||||
19323|Wallumbilla Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19323|Wallumbilla Formation|42520|5|Briefly described|p6|||||||||
19323|Wallumbilla Formation|42634|6|Mentioned|Table 8 P34|||||||||
19323|Wallumbilla Formation|42637|4|Described|p10, 23|||||||||
19323|Wallumbilla Formation|42673|5|Briefly described|Fig.2, P184|||||||||
19323|Wallumbilla Formation|42746|6|Mentioned|Fig.6 P8|||||||||
19323|Wallumbilla Formation|42749|5|Briefly described|p31|||see also Fig.2 p27.||||||18-DEC-06
19323|Wallumbilla Formation|42804|5|Briefly described|p115|||||||||
19323|Wallumbilla Formation|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Siltstone, porcellanite, sandstone; marine fossils.  Geological province: Amadeus Basin.||||||23-JAN-08
19323|Wallumbilla Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
19323|Wallumbilla Formation|43000|5|Briefly described|p114|||see also Fig.5,p112||||||
19323|Wallumbilla Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19323|Wallumbilla Formation|43004|5|Briefly described|Table 1,p179|||||||||
19323|Wallumbilla Formation|43083|5|Briefly described|p185|Cretaceous|Cretaceous|Argillaceouis deposits.||||||17-JUN-09
19323|Wallumbilla Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19323|Wallumbilla Formation|43114|5|Briefly described|p14|||||||||
19323|Wallumbilla Formation|43122|5|Briefly described|p25|||see also Fig. 2.||||||
19323|Wallumbilla Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43287|5|Briefly described|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|43404|14|Not recorded|Table p11||Cretaceous|||||||
19323|Wallumbilla Formation|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
19323|Wallumbilla Formation|43591|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|43602|4|Described|191|||In the Eromanga Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|43625|6|Mentioned|p48,74|||||||||
19323|Wallumbilla Formation|43630|6|Mentioned|p69, fig.4|||||||||
19323|Wallumbilla Formation|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|44031|14|Not recorded|p3,8,9,11,12||Cretaceous|||||||
19323|Wallumbilla Formation|44034|4|Described|Tb.2,p2,5,7-10,Fig.1|||||||||
19323|Wallumbilla Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44082|6|Mentioned|p3,4,6,8,10-30,Tb.34||Early Cretaceous|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
19323|Wallumbilla Formation|44091|14|Not recorded|p60,63||Cretaceous|||||||
19323|Wallumbilla Formation|44099|14|Not recorded|Map Legend||Early Cretaceous|(Rolling Downs Group)||||||
19323|Wallumbilla Formation|44112|6|Mentioned|p82|||||||||
19323|Wallumbilla Formation|44133|5|Briefly described|p104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|44308|14|Not recorded|p11,|||||||||
19323|Wallumbilla Formation|44376|14|Not recorded|p3|||||||||
19323|Wallumbilla Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44637|14|Not recorded|p287-291||Cretaceous|||||||
19323|Wallumbilla Formation|44807|14|Not recorded|p9|||Correlated with Blackdown Formation.||||||
19323|Wallumbilla Formation|45022|6|Mentioned|p111|Albian|Aptian|||||||
19323|Wallumbilla Formation|45071|6|Mentioned|p79|||||||||
19323|Wallumbilla Formation|45110|6|Mentioned|p24|||See also Table 18.||||||
19323|Wallumbilla Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
19323|Wallumbilla Formation|45145|3|Fully described|Table 5|||||||||
19323|Wallumbilla Formation|45161|6|Mentioned|p67|||||||||
19323|Wallumbilla Formation|46791|4|Described|p44|||||||||
19323|Wallumbilla Formation|46881|6|Mentioned|p198|||||||||
19323|Wallumbilla Formation|46902|6|Mentioned|p36|||||||||
19323|Wallumbilla Formation|46937|6|Mentioned|Fig.10|||||||||
19323|Wallumbilla Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19323|Wallumbilla Formation|46984|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|47042|6|Mentioned|p171|||||||||
19323|Wallumbilla Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|48919|6|Mentioned|p71|||Cretaceous. See also P72||||||
19323|Wallumbilla Formation|48920|3|Fully described|p58|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|48951|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19323|Wallumbilla Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19323|Wallumbilla Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|50332|5|Briefly described|p22, p78|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
19323|Wallumbilla Formation|50627|5|Briefly described|Map legend|Cretaceous|Cretaceous|Clay-rich mudstone, silty mudstone, sandy siltstone, and sandstone.||||||
19323|Wallumbilla Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Mudstone and quartz-poor sandstone, minor glauconitic sandstone.||||||
19323|Wallumbilla Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, minor labile and galuconitic sandstone, limestone.||||||
19323|Wallumbilla Formation|60281|5|Briefly described|p27|Early Cretaceous|Early Cretaceous|Geological Province: Clarence-Moreton Basin, Cecil Plains Sub-basin.||||||20-JAN-05
19323|Wallumbilla Formation|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Overlies Gilbert River Formation. Overlain by Toolebuc Formation. Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies: Coffin Hill Member (Gilbert River Formation). Mudstone and siltstone, minor sandstone. Geological Province: Carpentaria Basin.||||||20-AUG-04
19323|Wallumbilla Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Silty and sandy claystone, mudstone and siltstone, calcareous concretions; minor glauconitic sandstone. Geological Province: Laura Basin.||||||18-AUG-04
19323|Wallumbilla Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, siltstone.||||||
19323|Wallumbilla Formation|60524|5|Briefly described|p486 Fig. 1, p488|Albian|Aptian|Marine deposits; contains Viviparidae fossils.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Toolebuc Formation. Lateral to Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
19323|Wallumbilla Formation|61014|6|Mentioned|p533 Fig.2, p539. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wyandra Sandstone Member. Is overlain by Allaru Mudstone.||
19323|Wallumbilla Formation|61312|4|Described|p64, p67 Fig. E5, p73-74|Early Cretaceous|Early Cretaceous|Of Rolling Downs Gp. Marine sediment sequence of mudstone and siltstone, with limestone, minor lenticular sandstone, and intraformational conglomerate. Overlies Cadna-owie Fm.; overlain by Toolebuc Fm in Qld. Thickness: 300m. Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, siltstone, minor sandstone, coal, conglomerate. Overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19323|Wallumbilla Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
19323|Wallumbilla Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
19323|Wallumbilla Formation|62029|5|Briefly described|p15|Cretaceous|Cretaceous|Siltstone and shale - impermeable and acts as reservoir seal. See also Fig. 4.||||||14-APR-08
19323|Wallumbilla Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
19323|Wallumbilla Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Formation.||
19323|Wallumbilla Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
19323|Wallumbilla Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~113-~98Ma. Geological Province: Northern Gulf of Carpentaria.||||||01-MAR-10
19323|Wallumbilla Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|63979|1|Redefined|p48, Fig. 44|Albian|Barremian|Lower part of Wilgunya Subgp.Equates to Bulldog Shale, Coorikiana Sst.+lower part of Oodnadatta Fm in SA. Informally subdiv.into lower+upper Wallumbilla Fm.Contains Doncaster +Coreena Members.Conformable on Cadna-owie Fm. Thickness:350m.Detailed lith.||||||03-DEC-18
19323|Wallumbilla Formation|64048|5|Briefly described|p64 Tb. 2|Early Cretaceous|Early Cretaceous|Contains the Coreena Member. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Unit in Marree Subgroup.||Eromanga Basin: underlies Toolebuc Formation; overlies Cadna-owie Formation. Surat Basin: underlies the Surat Siltstone, overlies the Bungil Formation.||11-DEC-15
19323|Wallumbilla Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|64820|5|Briefly described|pS6 Fig. 4|Barremian|Albian|Of the Rolling Downs Group. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
19323|Wallumbilla Formation|64856|3|Fully described|p79, p98-101|Albian|Aptian|Named and defined in the Surat Basin by Vine et al. (1967), with the type section in Wallumbilla Creek, near Roma. Also in Eromanga Basin. Contains Doncaster and Coreena Members. Conformably overlies Bungil Formation. Age from pollen assemblages (units APK3, 4). Mudstone, siltstone, concretionary limestone, minor lenticular sandstone, conglomerate. Up to 475m thick.|| ||||29-NOV-17
19323|Wallumbilla Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19323|Wallumbilla Formation|65112|6|Mentioned|Fig 11 p324; Fig 16 p 328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies the Bungil Formation; underlies the Surat Siltstone.||22-MAR-12
19323|Wallumbilla Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Bungil Formation, Surat Siltstone.||||||
19323|Wallumbilla Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
19323|Wallumbilla Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Includes Coreena Member, Doncaster Member. Underlies the Surat Siltstone, Overlies the Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|65119|5|Briefly described|p503, 504, fig 7-8 p514, Fig 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Marine shelf deposits of siltstone, mudstone and fine sandstone. Age: 111-117 Ma. Fission Track age: 87-109 Ma.||||||07-MAR-12
19323|Wallumbilla Formation|65238|5|Briefly described|p7 Fig. 8, p14 Fig. 17|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
19323|Wallumbilla Formation|65384|6|Mentioned|S116, S118|||In Surat Basin? Includes Doncaster Member.||||||
19323|Wallumbilla Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Cadna-owie Formation. Overlain by Toolebuc Formation.||||||08-MAR-12
19323|Wallumbilla Formation|65489|5|Briefly described|p49, p55-56, p58, p61, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 450m thick. Regional seal.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Rolling Downs Group.|Includes Doncaster, Coreena, Jones V and Ranmoor Members.|||
19323|Wallumbilla Formation|66623|3|Fully described|p239, pp242-245, pp256-259. |Albian|Aptian|Previously known as the Blackdown Formation in Queensland. c.360 m thick. Contains a wide range of fossils. Shoreline to deeper marine environment. Outcrops as low rolling hills. Hosts opals at White Cliffs; possible heavy mineral (magnetite and zircon) strandlines locally.||Unit in Rolling Downs Group.|Includes Coreena and Doncaster Members.|Conformably, but sharply overlies Wyandra Sandstone Member. Coreena Member is gradationally overlain by Allaru Mudstone. Doncaster Member disconformably overlies Cadna-owie Formation.|Muddy sandstone and siltstone with local large spherical calcareous concretions; black shale and minor sandstone with abundant dropstone boulders; pyritic and bioturbated mudstone, claystone and shale; calcareous and glauconitic sandstones.|05-JUN-13
19323|Wallumbilla Formation|66915|4|Described|p1-2, 4-6, p9, p11 Fig.7, p12, p16, p18|Cretaceous|Cretaceous|Carpentaria, Eromanga and Surat Basins. Base of Wallumbilla Formation (the "C-Horizon") and correlatives is the major bounding surface of the Great Artesian Basin.||Basal Rolling Downs Group|Coreena Member, Doncaster Member|Overlies Wyandra Sandstone Member (Cadna-owie Formation), Gilbert River and Bungil Formations.|Marine muds.|12-JAN-17
19323|Wallumbilla Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67133|5|Briefly described|p2, p5, p17-19|Early Cretaceous|Early Cretaceous|Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (27-52%), feldspars (20-30%) with plagioclase dominant, minor (<8%) kaolinite and significant (13-26%) mixed-layer clays, mainly illite.|||Doncaster and Coreena Members.||Siltstones and mudstones with minor sandstones.|
19323|Wallumbilla Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Cadna-owie Formation. Is overlain by Allaru Mudstone.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Easter Monday Formation.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67323|5|Briefly described|p86-87, p92 Fig.12.2, p93, p94 Fig.12.4|Early Cretaceous|Early Cretaceous|See also GIS attrib tbl, Solid Geology Map, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Marine sediments.|||Includes Ranmoor Member.|Overlies Cadna-owie and Gilbert River Formations and Longsight Sandstone. Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|67402|4|Described|p26, p26 tbl RRM4, p29|Albian|Aptian|Eromanga Basin. Deposited in a transgressive marine environment which was followed by paralic and fluvial deposition. Ranges from 200 to over 350m thick in the Eromanga Basin and up to 600m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. Misspelt as Wullumbilla on p265. See also p29 fig PSA4, PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p120, P123, p146 fig SRT3, p148, p156, p176, p177, p179 fig CRP/KRM6, p181, p265.||Rolling Downs Group||Overlies the Cadna-owie Formation and Gilbert River Formation. Overlain by the Allaru Mudstone and Toolebuc Formation.|Consists primarily of marine mudstone interbedded with sandy mudstone, siltstone, shale and limestone.|
19323|Wallumbilla Formation|67561|5|Briefly described|p51-60, p62 Fig.11, p67, p68|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||||Correlative of the Bulldog Shale.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
19323|Wallumbilla Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Rolling Downs Group.||Underlain by Bungil Formation.||
19323|Wallumbilla Formation|67784|6|Mentioned|p25, p26, p28-29, p31, p32|||185-253m thick. Northern Eromanga Basin.||Wilgunya Subgroup.|Includes Doncaster Member, Jones Valley Member, Ranmoor Member, Coreena Member|Overlies Gilbert River Formation, overlain by Toolebuc Formation||08-FEB-18
19323|Wallumbilla Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68004|6|Mentioned|p175.|||A seal for reservoirs in the Hooray and Mooga Sandstones.||||||
19323|Wallumbilla Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group|Includes Coreena and Doncaster Members.|Overlies Bungil Formation. Is overlain conformably by Surat Siltstone.|Sandstone, claystone, siltstone and mudstone.|22-NOV-13
19323|Wallumbilla Formation|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|||
19323|Wallumbilla Formation|68206|5|Briefly described|p31-33|Aptian|Aptian|Carpentaria, Eromanga Basins.|||Doncaster, Jones Valley, Ranmoor Members.|Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19323|Wallumbilla Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.||||Conformably underlain by the Coffin Hill Member, Gilbert River Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Eromanga, Laura and Carpentaria Basins.||Unit in Rolling Downs Group.||Is overlain conformably by Griman Creek Formation and Toolebuc Formation.||
19323|Wallumbilla Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68593|5|Briefly described|p4, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.|||Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.|Siltstone, mudstone, minor conglomerate, rare coal.|
19323|Wallumbilla Formation|68731|6|Mentioned|pp209-211|||||||||
19323|Wallumbilla Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Aptian|Barremian|Eromanga Basin (NE). Marine to coastal paralic and shallow marine.||Of the Rolling Downs Group.|Includes Coreena Member and Doncaster Member.|||16-JAN-17
19323|Wallumbilla Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, p296, p298|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent to the Bulldog Shale Formation. Parallic to marine sediments. Contains ubiquitous disseminated pyrite.||Of the Rolling Downs Group.|||Consist of pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
19323|Wallumbilla Formation|68901|5|Briefly described|p7 Fig. ii|Upper Cretaceous|Lower Cretaceous|Eromanga Basin.||Rolling Downs Group|||Mudstone, siltstone, sandstone; calcareous in part.|27-SEP-18
19323|Wallumbilla Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Aptian|Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Aptian|||||||
19323|Wallumbilla Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. Contains good TOC for hydrocarbon generation.||Rolling Downs Group||Overlies the Gilbert River Formation. Overlain by the Toolebuc Formation.|Lithic glauconitic sandstones, siltstone, claystone and limestone.|
19323|Wallumbilla Formation|69377|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous||||||Mudstone and siltstone with calcareous concretions|
19323|Wallumbilla Formation|69379|5|Briefly described|map legend|Cretaceous|Cretaceous||||Doncaster Member|||
19323|Wallumbilla Formation|69454|6|Mentioned|p38:3, 13|||Eromanga Basin. Potential seal for Cadna-owie Formation sandstone reservoirs.||||||12-JUL-16
19323|Wallumbilla Formation|69455|5|Briefly described|p39:4 Fig.39.3; 39:14-15|Early Cretaceous|Early Cretaceous|Provides a seal to Gilbert River Formation sandstone reservoirs in the offshore Western Gulf Sub-basin. Organic-rich shale is a possible source rock.||||||12-JUL-16
19323|Wallumbilla Formation|69457|3|Fully described|p41:2-3; 41:5 Fig.41.4; 41:6-10, 14-16|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga, Carpentaria and Surat Basins. Mostly subsurface; outcrops form mesas, buttes or low rounded duricrusted hills. Shallow-marine, nearshore to marginal marine, minor non-marine deposits. 143m to over 350m thick. Equivalent to the succession comprising Bulldog Shale, Coorikiana Sandstone and lower part of Oodnadatta Formation. The name Bulldog Shale has previously (and inappropriately) been used to describe this Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals. May seal Cadna-owie Formation reservoirs.||Wilgunya Subgroup.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Cadna-owie Formation conformably, and Algebuckina Sandstone disconformably/unconformably. Is overlain conformably by Toolebuc Formation.|Mudstone and siltstone; minor thin intervals of fine sandstone and limestone. Locally calcareous, and may contain glauconite; shell fragments common in places. Locally silicified to porcellanite. Contains diverse fossil assemblages.|12-JUL-16
19323|Wallumbilla Formation|69582|5|Briefly described|p22, p25-p26, p29, p36, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga and Surat basins. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlain by the Toolebuc Formation and the Surat Siltstone. Overlies the Bungil Formation and the Cadna-owie Formation.|Sandstone.|
19323|Wallumbilla Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69594|4|Described|p518-519, p521-522, p526, p528-530, p534|Aptian|Barremian|See also p538, p540, p550, p573. Vine et al. (1967). Carpentaria, Eromanga, Laura and northern Surat Basins. Much of the upper part was previously known as Blackdown Formation (Laing and Power, 1959; Woods, 1961). Up to 475m thick. Contains a rich marine fauna (listed). Members not always discernible. RELATED UNITS (continued): Equivalent to Rolling Downs Group in the Laura Basin, the Roma Formation and lower part of overlying Tambo Formation.||Wilgunya Subgroup.|Coreena, Doncaster, Jones Valley, Ranmoor, Trimble Members.|Conformably overlies Gilbert River, Cadna-owie, Bungil Formations, Longsight Sandstone, Ronlow and Helby beds. Is overlain by Toolebuc Formation, Surat Siltstone and Allaru Mudstone. See COMMENTS.|Volcanogenic. Dominated by thick successions of sporadically nodular siltstone with lesser glauconitic sandstone, volcanic crystal-lithic sandstone and silty limestone.|
19323|Wallumbilla Formation|69673|5|Briefly described|p155 fig 127, p156, p159, p161|Cretaceous|Cretaceous|||Wilgunya Subgroup|Includes Doncaster Member, Coreena Member|Overlies Mount Anna Sandstone Member, Cadna-owie Formation overlain by Toolebuc Formation, correlated with Bulldog Shale|Mudstone, shale and siltstone with minor thin interbeds of fine sandstone and limestone.|
19323|Wallumbilla Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous||||Includes Doncaster and Coreena Members.|||
19323|Wallumbilla Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|69946|3|Fully described|p19, p21-25, p56-57, p94|Early Cretaceous|Early Cretaceous|Vine et al. (1967); formerly Roma Formation, used by the petroleum industry. Type section is 'Wallumbilla Creek, from Wallumbilla Township south for 12 miles [19.3km]'. Distribution is by definition controlled by Toolebuc Formation: where absent, Bulldog Shale is used. Lithology is identical to Bulldog Shale. Up to 596m thick. Early Aptian-Albian. Wireline log correlations.||||Conformably overlies Cadna-owie Formation. Is overlain conformably by Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone. Local pebbly and muddy diamictite containing metamorphic and sedimentary clasts.|
19323|Wallumbilla Formation|69947|5|Briefly described|p9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation).|Thick, fossiliferous mudstones and siltstones.|
19323|Wallumbilla Formation|69948|6|Mentioned|p4; Figs.4.2, 18|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.|Marine shales.|
19323|Wallumbilla Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Mudstone, siltstone, sandstone; calcareous in part.|
19323|Wallumbilla Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Early Cretaceous|Georgetown region.||||||
19323|Wallumbilla Formation|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup.|||Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone and siltstone with calcareous concretions.|20-JAN-22
19323|Wallumbilla Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|Includes Coreena Member, Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice rafted erratics.|
19323|Wallumbilla Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Rolling Downs Group|Includes Coreena Member, Doncaster Member.|||
19323|Wallumbilla Formation|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70720|6|Mentioned|p24-25|Early Cretaceous|Early Cretaceous||||Doncaster Member.|||
19323|Wallumbilla Formation|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p28|Early Cretaceous|Early Cretaceous|See also p30-31, p33, p79-80, p82, p85-88, p111-112, p117. Vine et al. (1967). The most widely distributed marine unit within the Great Australian Superbasin: Eromanga, Carpentaria, Laura and parts of Surat Basins. Varying thicknesses given from wells. Aptian to Albian age. Hydrochemistry mentioned; hydrostratigraphic properties. Equivalent to Bulldog Shale and Oodnadatta Formation.||Rolling Downs Group.|Doncaster, Coreena Members.|Overlies Cadna-owie and Bungil Formations, Hooray Sandstone and Drildool beds. Is overlain by Toolebuc Formation or Surat Siltstone; locally by Winton Formation (conformably).||
19323|Wallumbilla Formation|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 450m thick. Deposited in open marine transgressive to regressive marine shoreface environments.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Albian.|||Coreena, Doncaster Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|70860|6|Mentioned|p281|||Great Artesian Basin.|||Coreena, Doncaster, Ranmoor, Jones Valley, Members.|||
19323|Wallumbilla Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29|||First described by Isbell (1957). Eromanga Basin. 186m total thickness in Eulo 1 borehole; it was not possible to differentiate the two Members in this borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||Rolling Downs Group.|Coreena and Doncaster Members.|Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Winton Formation.|Generally monotonous, glauconitic, marine, dark bluish-grey carbonaceous mudstone with some lignite plant fragments, some thin (estimated <1m) beds of siltstone and fine sandstone.|
19323|Wallumbilla Formation|71321|5|Briefly described|p15,27,65|Cenomanian|Cenomanian|Of Eromanga Basin. Previously known as Roma Formation. Regressivee depositional package following peak early Cretaceous marine transgression; marginal marine shoreface deposit.||||Equivalent to Bulldog Shale. Overlain by the Toolebuc Formation.||24-OCT-19
19323|Wallumbilla Formation|71342|3|Fully described|Ch4 p4, Ch4 p9, Ch4 p25|Albian|Aptian|Eromanga Basin. Formally defined by Vine et al (1967)  to replace the Roma Formation. Vine et al also defined the type section in "Wallumbilla Creek,from Wallumbilla Township south for 12 miles" in Queensland. This unit reaches a maximum thickness of 596m in Coonatie 1 in the Patchawarra Trough and 260m in the Poolowanna Trough. Age derived from palynology. Interpreted to have been deposited in a shallow epicontinental sea at cold high latitudes as debris flows. Spore-pollen zone is given in Ch5 p57. See also Ch5 p22, Ch5 p24-p25, Ch5 p30, Ch5 p57, Ch6 p8-p9, Ch7 p9, Ch7 p13, Ch10 p17, Ch11 p4-p5, Ch12 p12, Ch12 p14.||||Conformably overlies the Wyandra Sandstone Member (Cadna-owie Formation). Conformably overlain by the Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone.|
19323|Wallumbilla Formation|71382|5|Briefly described|p4, p13, p16-p17, p19-p20|||Intersected in GSQ Julia 1 from 199.87m-310.49m for a total of 110.62m thickness. Temp log and stratlog are provided. Lithology is described in detail on p20. See also p23, p25, p27, App 3, 4.||||Overlies the Hooray Sandstone. Overlain by the Toolebuc Formation.|Interbedded mudstone and sandstone with minor calcareous mudstone.|
19323|Wallumbilla Formation|71855|4|Described|p2, p4-p6, p9-p10, p13|Jurassic|Jurassic|Eromanga and Carpentaria basins. In places the contact with the overlying Toolebuc Formation is disconformable or faulted. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p15, p27, p33-p35, p50, p52-p53, p56-p57, p75.||||Conformably (gradationally) overlain by the Toolebuc Formation.|Glauconitic, smectite-rich mudstone, siltstone or fine-grained sandstone.|
19323|Wallumbilla Formation|71863|5|Briefly described|p4-p9|Albian|Aptian|Eromanga and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group|Includes the Doncaster Member and the Coreena Member.|Overlies the Gilbert River Formation, Helby beds and the Cadna-owie Formation. Conformably overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|71864|4|Described|p8, p10, p13-p14, p16-p20|||Intersected in GSQ Eulo 2 borehole between 23-51m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as glauconitic marine siltstones and claystones. Gamma log characteristics and magnetic susceptibility is provided.||Rolling Downs Group|Includes the Coreena Member and the Doncaster Member.|Overlain by the Winton Formation. Overlies the Waihora Volcanics.|Dark blue to light grey siltstone with a distinctive layer producing carbonaceous flecks and a fine quartzose sandstone layer in addition to mudstone.|
19323|Wallumbilla Formation|71890|6|Mentioned|p7|||Surat Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72297|5|Briefly described|p742, p746, p753|||Eromanga Basin. Acts as a regional seal. Potential hydrocarbon source rocks.|||Ranmoor Member.|Is overlain conformably by the Toolebuc Formation.|Shales and mudstones.|
19323|Wallumbilla Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||Rolling Downs Group.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Wyandra Sandstone Member (Cadna-owie FZ); Gilbert River and Bungil FZs; Ronlow, Helby, Albany Pass and Drildool beds. Is overlain by Toolebuc FZ or Surat Siltstone.||
19323|Wallumbilla Formation|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.||||||
19323|Wallumbilla Formation|72914|5|Briefly described|p12, p14, p16, p18, p20-21, p29, App. I|Cretaceous|Cretaceous|In Tongo 1 [borehole], the unit is semi-monotonous consisting chiefly of marine siltstone and claystone, but can occasionally has washes of coarser-grained quartzose sediments derived from local basement highs. Natural gamma emissions are relatively subdued and monotonous.||||Underlain by the Wyandra Sandstone Member (Cadna-owie Formation).|Marine siltstone and claystone with occasional washes of coarser-grained quartzose material.|
19323|Wallumbilla Formation|72915|6|Mentioned|p16, p19, p27, p39 App E, App I|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group, and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Mineralogical changes from clay-rich to quartz-rich are reflected in natural gamma emissions [data]. Relatively non-magnetic in Congararra 1. No groundwater was made from this unit in Congararra 1.||||||
19323|Wallumbilla Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73083|6|Mentioned|p62-63|Cretaceous|Cretaceous|||||Overlain by the Toolebuc Formation.|Mudstone and siltstone.|
19323|Wallumbilla Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: p. 119, 146, 151-152, 168-172, 177-178, 191.||||||
19323|Wallumbilla Formation|73137|6|Mentioned|p6, p81|Cretaceous|Cretaceous|Carpentaria Basin. Intersected in drill hole GIDPDS5.||||||08-OCT-22
19323|Wallumbilla Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Gilbert River Formation. Overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous||||Doncaster Member||Includes interbedded sandy/silty claystone and interbedded fine sandstones.|
19323|Wallumbilla Formation|73249|5|Briefly described|p319, p321, p323|Albian|Aptian|North and east of the Eromanga Basin [shown as within the Eromanga Basin on p319 Fig.2]. Laterally equivalent to the Bulldog Shale.||||Lateral equivalent to the Bulldog Shale, overlies the Cadna-owie Formation, underlies the Toolebuc Formation.|Siltstone and mudstone dominated.|
19323|Wallumbilla Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Eromanga Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
19323|Wallumbilla Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73479|5|Briefly described|p156 Fig.2, p159, p163, p164 Fig.7, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine and shoreface depositional environment.|ca 125-104 Ma|||Overlies Wyandra Sandstone Member, underlies Toolebuc Formation||
19323|Wallumbilla Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19332|Walsh Bluff Volcanics|23423|4|Described|p305 Table 7.3||Early Permian|Also see p237. Overlain by Atherton Basalt (unconformable); Underlain by Atlanta, Saint Patrick Hill and Lass O'Gowrie Granites. Kennedy Igneous Province.||||||23-APR-09
19332|Walsh Bluff Volcanics|23506|5|Briefly described|Map Legend||Early Permian|||||||
19332|Walsh Bluff Volcanics|23513|5|Briefly described|Map legend||Permian|Palaeozoic Volcanic No. V79. I-Type.||||||
19332|Walsh Bluff Volcanics|23616|5|Briefly described|Table 3 p44||Early Permian|Age: early Permian? Unconfrm on or faulted against Atlanta, St Patrick Hill and Lass O'Gowrie Granites & Hodgkinson Fm rocks. Cut by felsic dykes of Parasta Dyke Swarm & early Permian Watsonville Granite. Koolmoon Volcanic Gp. Thickness 600m.||||||
19332|Walsh Bluff Volcanics|29794|6|Mentioned|Fig.4|||||||||
19332|Walsh Bluff Volcanics|29820|6|Mentioned|p449|||||||||
19332|Walsh Bluff Volcanics|30505|4|Described|p4|||See alsp P5,6,7. Early Permian age||||||
19332|Walsh Bluff Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19332|Walsh Bluff Volcanics|31832|6|Mentioned|Table 6|||||||||
19332|Walsh Bluff Volcanics|33205|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19332|Walsh Bluff Volcanics|36563|6|Mentioned|p552|||||||||
19332|Walsh Bluff Volcanics|37613|6|Mentioned|p247|||See also P247 and Fig.1.||||||
19332|Walsh Bluff Volcanics|39252|6|Mentioned|Fig.11|||||||||
19332|Walsh Bluff Volcanics|39445|5|Briefly described|Table 7|||||||||
19332|Walsh Bluff Volcanics|40049|6|Mentioned|Fig.2|||||||||
19332|Walsh Bluff Volcanics|43060|5|Briefly described|Fig.4A-B|||||||||
19332|Walsh Bluff Volcanics|43259|4|Described|Appendix 1,p8.|Permian|Carboniferous|||||||
19332|Walsh Bluff Volcanics|43896|14|Not recorded|Map Legend|Permian|Carboniferous|||||||
19332|Walsh Bluff Volcanics|44246|5|Briefly described|Map Legend||Early Permian|||||||
19332|Walsh Bluff Volcanics|44296|14|Not recorded|Map Legend|Triassic|Permian|||||||
19332|Walsh Bluff Volcanics|45014|2|Defined|p31,48-52,Pl.13,38|Late Carboniferous|Early Carboniferous|Tb.1. (Probably Middle-Late Carboniferous)||||||
19332|Walsh Bluff Volcanics|45025|4|Described|p68|Permian|Carboniferous|||||||
19332|Walsh Bluff Volcanics|45065|4|Described|Table 4|||||||||
19332|Walsh Bluff Volcanics|45113|3|Fully described|p27|||Emphasis on petrography.||||||
19332|Walsh Bluff Volcanics|46845|6|Mentioned|Table 1|||||||||
19332|Walsh Bluff Volcanics|48976|4|Described|p67|||Isotopic data Table 18||||||
19332|Walsh Bluff Volcanics|60425|4|Described|p41, p44 Tb.3|Late Palaeozoic|Late Palaeozoic|Unconformable on or faulted against Atlanta + Lass O'Gowrie Granites + Hodgkinson Fm; unconformable under Atherton Basalt. Cut by Cherry Tree+Watsonville Granites. Age: ~275+/-23Ma, ~282+/-9Ma (Rb-Sr). Thickness:600m? Rhyolitic - detailed lith.included||||||07-FEB-11
19332|Walsh Bluff Volcanics|66180|5|Briefly described|pp279-280|Late Permian||||||Overlies the Hodgkinson Formation.|Felsic volcanics.|10-MAY-12
19332|Walsh Bluff Volcanics|68576|5|Briefly described|Q_11: p6, p17|Permian|Permian|Dimbulah area. A range-forming unit; part of the Kennedy Igneous Association.||||||
19332|Walsh Bluff Volcanics|72983|6|Mentioned|p1, p18|early Permian|early Permian|||||Cut by some felsic dykes of the Collins Weir Rhyolite.||
19368|Wandilla Formation|23799|6|Mentioned|p18|||Of the Curtis Island Group.||||||
19368|Wandilla Formation|24382|5|Briefly described|Map legend|Carboniferous|Carboniferous|Parent: Curtis Island Group||||||
19368|Wandilla Formation|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Curtis Island Group.||||||
19368|Wandilla Formation|24488|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
19368|Wandilla Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||
19368|Wandilla Formation|24490|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Curtis Island Group. Mudstone, arenite and chert.||||||04-SEP-08
19368|Wandilla Formation|24615|5|Briefly described|CD|Carboniferous|Late Devonian|[DCcw].  Mudstone, lithic sandstone, siltstone, jasper, chert, slate; local schist.||||||
19368|Wandilla Formation|29420|6|Mentioned|p98|||||||||
19368|Wandilla Formation|30451|3|Fully described|p8|||Lower ? Palaeozoic age.||||||18-AUG-08
19368|Wandilla Formation|30655|6|Mentioned|p5|||||||||
19368|Wandilla Formation|30692|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
19368|Wandilla Formation|30777|5|Briefly described|p417|||Discussed||||||
19368|Wandilla Formation|30811|6|Mentioned|p532|||||||||
19368|Wandilla Formation|30915|6|Mentioned|p98|||||||||
19368|Wandilla Formation|30916|6|Mentioned|p96|||||||||
19368|Wandilla Formation|31365|4|Described|p3|||Palaeozoic. Unit of Curtis Island Gp.||||||
19368|Wandilla Formation|31657|4|Described|p91|||See also p92, 100. Ordovician-Silurian.||||||12-NOV-15
19368|Wandilla Formation|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
19368|Wandilla Formation|31659|2|Defined|p19, p20-23|Early Paleozoic|Early Paleozoic|Max. thickness: >28,000ft. Mudstone, quartz greywacke, pale grey chert. See also Table 1.||||||07-NOV-08
19368|Wandilla Formation|32357|4|Described|Table 1|||||||||
19368|Wandilla Formation|32358|4|Described|Table 1|||||||||
19368|Wandilla Formation|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
19368|Wandilla Formation|33769|5|Briefly described|p150|||||||||
19368|Wandilla Formation|33774|3|Fully described|p63|||||||||
19368|Wandilla Formation|33879|6|Mentioned|p284|||||||||
19368|Wandilla Formation|34947|6|Mentioned|p360|||||||||
19368|Wandilla Formation|35006|6|Mentioned|p278|||||||||
19368|Wandilla Formation|35007|6|Mentioned|p77|||||||||
19368|Wandilla Formation|35053|5|Briefly described|p38|||||||||
19368|Wandilla Formation|35101|6|Mentioned|p19|||||||||
19368|Wandilla Formation|35266|6|Mentioned|p206|||||||||
19368|Wandilla Formation|36211|6|Mentioned|p267|||||||||
19368|Wandilla Formation|36333|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous.||||||18-AUG-08
19368|Wandilla Formation|36488|4|Described|p3|||||||||
19368|Wandilla Formation|36528|6|Mentioned|p170|||See also Fig.4||||||
19368|Wandilla Formation|36576|6|Mentioned|p611|||||||||
19368|Wandilla Formation|37453|5|Briefly described|p313|||||||||
19368|Wandilla Formation|38081|5|Briefly described|Table 1|||||||||
19368|Wandilla Formation|38143|6|Mentioned|p13|||||||||
19368|Wandilla Formation|38391|6|Mentioned|p6|||||||||
19368|Wandilla Formation|38406|5|Briefly described|p9|||||||||
19368|Wandilla Formation|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous.||||||18-AUG-08
19368|Wandilla Formation|39445|5|Briefly described|Table 6|||||||||
19368|Wandilla Formation|39632|6|Mentioned|p208|||||||||
19368|Wandilla Formation|40475|6|Mentioned|p2|||||||||
19368|Wandilla Formation|40623|5|Briefly described|p85|||See also p109.||||||12-NOV-15
19368|Wandilla Formation|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
19368|Wandilla Formation|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
19368|Wandilla Formation|41738|6|Mentioned|p166|||||||||
19368|Wandilla Formation|41778|6|Mentioned|Table 1|||||||||
19368|Wandilla Formation|41922|4|Described|Table 1, P11|||||||||
19368|Wandilla Formation|42143|5|Briefly described|p592|||||||||
19368|Wandilla Formation|42547|4|Described|p53|||||||||
19368|Wandilla Formation|42660|4|Described|p23 p169|||||||||
19368|Wandilla Formation|42901|5|Briefly described|p404|||see also Fig.12 p412.||||||12-NOV-15
19368|Wandilla Formation|43008|5|Briefly described|map legend|||||||||
19368|Wandilla Formation|45107|6|Mentioned|p6|||||||||
19368|Wandilla Formation|50190|6|Mentioned|p28|||||||||
19368|Wandilla Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of the Curtis Island Group.||||||
19368|Wandilla Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Of Curtis Island Group.||||||28-MAY-08
19368|Wandilla Formation|60557|5|Briefly described|p23|Early Carboniferous|Late Devonian|Of the Curtis Island Group. Consists mainly of mudstone and sandstone and thick-bedded chert bands.||||||05-SEP-14
19368|Wandilla Formation|61035|5|Briefly described|p14|||Geological Province: Wandilla Province. Consists of mudstone, volcanolithic sandstone, siltstone, jasper + chert.||||||07-FEB-11
19368|Wandilla Formation|63748|6|Mentioned|p15|Carboniferous|Carboniferous|In the Wandilla Province of Central Queensland.||||||07-FEB-11
19368|Wandilla Formation|63821|5|Briefly described|p15, p34, p38|Carboniferous|Early Carboniferous|Of Curtis Island Group. Max.depositional age: 337.5+/-2.3Ma and 350.4+/-2.1Ma. Tightly folded sequence of fine grained siliciclastic sediments and metasediments. Contains crinoids and radiolaria. Geological province: Wandilla Province - Coastal Block||||||07-FEB-11
19368|Wandilla Formation|64398|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of the Curtis Island Group. Mudstone, lithic sandstone (locally containg silicified oolites), siltstone, jasper, chert, slate; local schist. Subunits of possiblely chert and maif volcanics; rdige-forming, magnetic units.||||||14-AUG-08
19368|Wandilla Formation|64399|5|Briefly described|Map legend|Carboniferous|Late Devonian|Of Curtis Island Group. Comprises predominantly mudstone, lithic sandstone (locally ccontaining silicified oolites), silstone, jasper, chert. slate with local schist; and a subordinate unit of chert or quartzite which is resistant and ridge-forming.||||||
19368|Wandilla Formation|65380|5|Briefly described|p658, 660, 662-665, 671-672, 674||Pennsylvanian|Western Coastal Block, New England Orogen. Derived from dacitic to rhyolitic volcanics. Maximum depositional age from detrital zircon: 328+/-4 Ma, 316 +/- 3 Ma.||||||03-SEP-18
19368|Wandilla Formation|67203|5|Briefly described|p6-7|Early Carboniferous|Late Devonian|Forms basement in W side of Bobby Range in the Boxvale-Dalga Road area.|||||Fine-grained sandstones and siltstones.|
19368|Wandilla Formation|68008|3|Fully described|p50,p103, p107, p109, p111-113, p115-120|Early Carboniferous|Early Carboniferous|See also p186, p199, p217, p270, p273, p279, p291, p297, p329, p416-418, p428, p462, p465, p480, p482. Forms sharp ridges. Deep basinal deposits. Part of the Wandilla terrane. Is faulted against Channer Creek beds. Intruded by Miriam Vale and Riverston Granodiorites, Norton Tonalite, Mount Hedlow Trachyte, and Castletower, Molangul Granites. A deeper-water equivalent of Rockhampton Group. Structure and its timing discussed. Ooids were derived from the Rockhampton Group. Age from crinoid stem. Minor phosphatic and even less Mn mineralisation. Hosts the mottled and pallid zones of a laterite profile.||Curtis Island Group.||Overlies and is faulted against Doonside Formation; underlies and is faulted against Shoalwater Formation. Is overlain unconformably by Bobby Volcanics and Calliope beds. See Comments.|With the Doonside Formation, constitutes the Wandilla terrane: mudstone, greywacke, chert, greenstone and tuff; largely a lenticular melange.|
19368|Wandilla Formation|68421|5|Briefly described|Map Legend|Carboniferous|Late Devonian|Coastal Subprovince, Wandilla Province.||||Conformably overlain by the Shoalwater Formation.|Mudstone, lithic sandstone (locally containing silicified oolites), siltstone, jasper, chert, slate, local schist.|
19368|Wandilla Formation|68679|5|Briefly described|p317-319, p338, p426, p451, p469|Mississippian|Mississippian|Coastal Subprovince, Wandilla Province, New England Orogen. Forms a discontinuous belt >240km long and up to 20km wide. Estimated thickness of 10-16km is certainly an exaggeration due to fault repetition. The chert lenses form prominent ridges, esp. on Curtis Island. Oolitic sandstones resemble, and were sourced from, parts of the Rockhampton Group. Coeval with Rockhampton Group. Contains minor phosphatic and lesser manganiferous mineralisation; veins of variscite and metavariscite. Deformations described.||Curtis Island Group.||Is faulted against and locally overlies Doonside Formation. Is overlain transitionally by Shoalwater Formation. Is correlated with the Texas beds. Is intruded by Pyri Pyri Granite.|Mainly rhythmically interbedded mudstone and graded sandstone derived from intermediate to felsic volcanics. Volcaniclastic sandstones were deposited as turbidites. Large chert lenses. Has an interval with calcareous or silicified ooids.|
19368|Wandilla Formation|69594|6|Mentioned|p560|||||||Is intruded by Goondicum Gabbro.||
19368|Wandilla Formation|73201|6|Mentioned|p619|||New England Orogen. Inboard of a subduction complex.|||||Volcaniclastic sandstones.|
19368|Wandilla Formation|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, accretionary complex.|||||Includes coarse-grained, quartz-poor, volcanic-lithic sandstone.|
19368|Wandilla Formation|73450|6|Mentioned|p9, p21, p36, p67|Early Carboniferous|Early Carboniferous|||||Intruded by Castletower Granite, Molangul Granite, Toondahra Granite, and Goondicum Gabbro.||
19432|Warang Sandstone|13516|6|Mentioned|p169 Fig 11|Middle Triassic|Middle Triassic|Galilee Basin||||||
19432|Warang Sandstone|22621|6|Mentioned|p204||Triassic|||||||
19432|Warang Sandstone|22937|6|Mentioned|fig1||Mesozoic|||||||
19432|Warang Sandstone|23318|5|Briefly described|p392 Fig. 1|Triassic|Triassic|||||||
19432|Warang Sandstone|23425|6|Mentioned|p391|||||||||
19432|Warang Sandstone|23430|4|Described|p519 Table 14.6|||Maximum thickness: <700 m.||||||10-JUN-15
19432|Warang Sandstone|23499|5|Briefly described|map legend|Triassic|Triassic|Galilee Basin.||||||
19432|Warang Sandstone|23505|5|Briefly described|Map legend||Triassic|||||||
19432|Warang Sandstone|23508|5|Briefly described|Map Legend||Triassic|||||||
19432|Warang Sandstone|23940|5|Briefly described|p917 Fig. 3|Triassic|Triassic|Geological Province: Mount Windsor subprovince.||||||
19432|Warang Sandstone|23952|5|Briefly described|p1176 Fig.1|Triassic|Triassic|Geological Province: Mount Windsor subprovince||||||
19432|Warang Sandstone|23982|6|Mentioned|p97 Appendix 13|||Geological Province: Great Artesian Basin.||||||
19432|Warang Sandstone|24071|5|Briefly described|p320|Triassic|Triassic|Geological Province: Galilee Basin.||||||
19432|Warang Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
19432|Warang Sandstone|29387|6|Mentioned|Table 3|||See also Table 4. Triassic.||||||
19432|Warang Sandstone|30102|6|Mentioned|p14|||See also p15.||||||
19432|Warang Sandstone|30151|4|Described|Table 3|||See also Fig.3||||||
19432|Warang Sandstone|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
19432|Warang Sandstone|30915|6|Mentioned|p99|||||||||
19432|Warang Sandstone|30916|6|Mentioned|p97|||||||||
19432|Warang Sandstone|31121|4|Described|p388|||||||||
19432|Warang Sandstone|32138|6|Mentioned|p393|||||||||
19432|Warang Sandstone|32490|4|Described|Table 1|||Lower Triassic.||||||10-FEB-09
19432|Warang Sandstone|32493|6|Mentioned|Map legend|Triassic|Triassic|||||||
19432|Warang Sandstone|32553|4|Described|p40|||||||||
19432|Warang Sandstone|33086|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper TriassicM - U||||||
19432|Warang Sandstone|33638|6|Mentioned|p8|||||||||
19432|Warang Sandstone|33644|6|Mentioned|Map legend|Late Triassic|Early Triassic|Lower to Upper? Triassic||||||
19432|Warang Sandstone|33648|5|Briefly described|p18|||Triassic.  Age data.||||||10-FEB-09
19432|Warang Sandstone|34091|5|Briefly described|Table 1|||Triassic.||||||10-FEB-09
19432|Warang Sandstone|34391|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
19432|Warang Sandstone|34409|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
19432|Warang Sandstone|35063|6|Mentioned|p80|||||||||
19432|Warang Sandstone|35304|6|Mentioned|Fig.1|||||||||
19432|Warang Sandstone|35322|6|Mentioned|p416|||||||||
19432|Warang Sandstone|35457|6|Mentioned|p633|||Also Fig.4 biostratigraphic relationships.||||||
19432|Warang Sandstone|35560|4|Described|p283|||||||||
19432|Warang Sandstone|35562|6|Mentioned|p295|||Stratigraphy||||||
19432|Warang Sandstone|36243|6|Mentioned|Table 5A|||||||||
19432|Warang Sandstone|36472|6|Mentioned|Map legend|Triassic|Triassic|||||||
19432|Warang Sandstone|36561|6|Mentioned|p542|||See also Fig.1.||||||
19432|Warang Sandstone|36921|6|Mentioned|p175|||See also Table 1.||||||
19432|Warang Sandstone|37451|6|Mentioned|Table 2|||||||||
19432|Warang Sandstone|37603|6|Mentioned|p444|||||||||
19432|Warang Sandstone|37610|6|Mentioned|Fig.3|||||||||
19432|Warang Sandstone|37764|6|Mentioned|Table 1|||||||||
19432|Warang Sandstone|38358|6|Mentioned|p21|||||||||
19432|Warang Sandstone|39261|6|Mentioned|Fig. 9|||||||||
19432|Warang Sandstone|39285|6|Mentioned|Fig. 2|||||||||
19432|Warang Sandstone|39445|5|Briefly described|Table 9|||||||||
19432|Warang Sandstone|39686|6|Mentioned|p69|||See also p73||||||
19432|Warang Sandstone|39735|6|Mentioned|p19|||||||||
19432|Warang Sandstone|39943|6|Mentioned|Table 7A|||||||||
19432|Warang Sandstone|40123|6|Mentioned|Table 2|||||||||
19432|Warang Sandstone|40375|6|Mentioned|p133|||||||||
19432|Warang Sandstone|40433|6|Mentioned|Fig.6|||||||||
19432|Warang Sandstone|40623|5|Briefly described|p88|||See also p110.||||||10-FEB-09
19432|Warang Sandstone|40634|6|Mentioned|p31|||||||||
19432|Warang Sandstone|40958|6|Mentioned|Table 1|||||||||
19432|Warang Sandstone|41116|5|Briefly described|Table 1|||||||||
19432|Warang Sandstone|41266|6|Mentioned|Fig.3|||||||||
19432|Warang Sandstone|41710|5|Briefly described|p222|||||||||
19432|Warang Sandstone|42061|6|Mentioned|p150|||||||||
19432|Warang Sandstone|42447|6|Mentioned|Fig.4|||||||||
19432|Warang Sandstone|42633|5|Briefly described|Table 1 P6|||||||||
19432|Warang Sandstone|43105|5|Briefly described|p13|||||||||
19432|Warang Sandstone|43687|6|Mentioned|Fig.1,p204|||||||||
19432|Warang Sandstone|43705|6|Mentioned|p14|||||||||
19432|Warang Sandstone|43812|6|Mentioned|Fig.3,p145|||||||||
19432|Warang Sandstone|43934|5|Briefly described|Map Legend||Triassic|||||||
19432|Warang Sandstone|44034|6|Mentioned|Tb.1,p3|||||||||
19432|Warang Sandstone|44081|5|Briefly described|p131||Early Triassic|Probably lower Triassic. Briefly described in French.||||||
19432|Warang Sandstone|44414|14|Not recorded|p114||Early Triassic|||||||
19432|Warang Sandstone|45073|6|Mentioned|p59|||Stratigraphic table||||||
19432|Warang Sandstone|45095|6|Mentioned|p63|||Refers Vine, Casey, Johnson (1964)||||||
19432|Warang Sandstone|45151|5|Briefly described|Table 10|||See also p15.||||||10-FEB-09
19432|Warang Sandstone|46881|6|Mentioned|Fig.7|||||||||
19432|Warang Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19432|Warang Sandstone|48908|14|Not recorded|Tb.1||Early Jurassic|||||||
19432|Warang Sandstone|48914|4|Described|p51|||See also p53. Lower Triassic.||||||10-FEB-09
19432|Warang Sandstone|48995|5|Briefly described|p72|||Age and thickness only described. See also Fig.3.||||||
19432|Warang Sandstone|49010|6|Mentioned|Fig.4|||Galilee Basin||||||
19432|Warang Sandstone|49011|6|Mentioned|Fig.3|||Galilee Basin||||||
19432|Warang Sandstone|60659|5|Briefly described|p21|Triassic||Fluviatile deposits; common cross-bedding. Geological Province: Galilee Basin.||||||07-FEB-11
19432|Warang Sandstone|63713|5|Briefly described|p1507 Fig.2, p1516, p1521|Middle Triassic|Middle Triassic|Koburra Trough and NE margin, Galilee Basin.||||Overlies Clematis Group. Is overlain by Moolayember Formation.||
19432|Warang Sandstone|64849|5|Briefly described|Map legend|Triassic|Triassic|Kaolinitic quartz sandstone, conglomerate, mudstone, variegated mudstone and siltstone.||||||
19432|Warang Sandstone|64856|6|Mentioned|p69, 72|||Equivalent to Rewan Group? In the Hughenden-Pentland area. Middle or upper part is correlated with Clematis Group.|| ||||31-JAN-13
19432|Warang Sandstone|65489|5|Briefly described|p144|Middle Triassic|Early Triassic|Lovelle Depression, Galilee Basin.||||Overlies Betts Creek Beds. Is overlain by Moolayember Formation.|Quartz-rich sandstones.|
19432|Warang Sandstone|66188|6|Mentioned|431|||||||||
19432|Warang Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Clematis Sandstone. Is unconformably overlain by Ronlow beds.||
19432|Warang Sandstone|67323|5|Briefly described|p84, p86, p93, p96|Middle Triassic|Early Triassic|Lovelle Depression, Galilee Basin. An aquifer.||||Unconformably overlies Betts Creek beds. Is overlain conformably by Moolayember Formation. Tentatively correlated with Rewan Formation and Clematis Sandstone.||
19432|Warang Sandstone|67402|6|Mentioned|p124 fig GLL1, p127 fig GLL5, p135, p138|Ladinian|Changhsingian|Galilee Basin.||||Overlies the Betts Creek beds. Overlain by the Moolayember Formation.||
19432|Warang Sandstone|68413|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably overlain by the Moolayember Formation. Conformably underlain by the Rewan Formation.|Kaolinitic quartz sandstone, conglomerate, variegated mudstone and siltstone.|
19432|Warang Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Galilee Basin.||||||
19432|Warang Sandstone|68731|5|Briefly described|pp200-202|Middle Triassic|Middle Triassic|Vine, Casey, and Johnson (1964). Laterally equivalent to the Dunda beds and Rewan Group. Unconformity between the Betts Creek beds and Warang Sandstone is supported by Palynology.||||Equivalent to the Rewan Group. Disconformably underlain by the Betts Creek beds. Overlain by the Moolayember Formation||
19432|Warang Sandstone|71265|5|Briefly described|p589|Olenekian|Olenekian|NE Galilee Basin.||||Unconformably overlies Betts Creek Group.||
19432|Warang Sandstone|71394|5|Briefly described|p1, p5, p7-p9, p18, p20 , p22-p24|Middle Triassic|Early Triassic|Galilee Basin. A field transect across this unit is provided and at each stop where it occurs it is described. This unit is medium and thick bedded and also cross-bedded.||||Overlain by the Blantyre Sandstone. Overlies the Betts Creek beds.|Light grey to white, coarse to very coarse-grained, poorly sorted, quartzose sandstone. Sandstone is medium bedded with common cross-bedding.|
19432|Warang Sandstone|71701|5|Briefly described|p155|Olenekian|Induan|Northeastern Area, Galilee Basin.||||Unconformably overlies the Betts Creek Group.||
19432|Warang Sandstone|71710|4|Described|p370 Fig 3, p383-384, p385 Fig 21, p387|Middle Triassic|Middle Triassic|Geological province: northern Galilee Basin margin; White Mountains||sequence 10.||Correlative to the upper Clematis Group and lower Moolayember Formation. Discomformably underlain by Betts Creek beds.||22-MAY-19
19432|Warang Sandstone|72088|4|Described|p8, p21, p23, p25, p30, p91, p94|Ladinian|Induan|Lovelle Depression, Galileee Basin. Defined in outcrop by Vine et al (1964) near the northeastern margin of the Galilee Basin. Well exposed in Porcupine Creek.||||Conformably overlain by the Moolayember Formation. Unconformably overlies the Betts Creek beds.|Pebbly, poorly sorted, kaolinitic quartzose to sub-labile sandstone with interbeds of argillaceous rocks. Minor conglomerate bands are also present and a few seams of dull pyritic coal.|
19432|Warang Sandstone|72298|5|Briefly described|p801|Jurassic|Triassic|Eromanga Basin (SA,QLD). Confined aquifers, generally producing flowing artesian water bores.||||Overlies Clematis Sandstone. Is overlain unconformably by Ronlow beds.||
19432|Warang Sandstone|73472|4|Described|p113, p115-122, p125, p129-131, App.1|Norian|Olenekian|Galilee Basin / Eromanga Basin. Large fluvial braidplain depositional setting. Probably diachronous across the northeastern part of the basin. Maximum thickness of ca 850 m (GSQ Hughenden 1-2R core). Stratigraphic extent within Porcupine Gorge was adjusted (ca 61 m thick). [See article for palynology].||||Underlain by Porcupine Gorge Formation [paraconformity]. Overlain by and interfingers with the Moolayember Formation. Equivalent to Rewan Formation and Moolayember Formation.|Dominantly homogeneous, white, kaolinitic, medium- to coarse-grained, trough cross-bedded sandstone with minor interbedded claystones or siltstones and rare conglomerate lenses.|
19432|Warang Sandstone|73570|6|Mentioned|p914, p915 Fig.4, p916, p919 Fig.6|Middle Triassic|Early Triassic|Galilee Basin.|||||Fluviatile.|
19458|Warendian Stage|31572|2|Defined|p5|Ordovician|Ordovician|||||||
19533|Warrina Park Quartzite|22498|6|Mentioned|Fig2 P235, Fig5|||||||||
19533|Warrina Park Quartzite|23031|5|Briefly described|28|||Geol province: Leichardt River Subprovince. Overlain by Moondarra Siltstone.||||||01-FEB-07
19533|Warrina Park Quartzite|23362|5|Briefly described|339|||||||||
19533|Warrina Park Quartzite|23393|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of Mount Isa Group.||||||07-NOV-08
19533|Warrina Park Quartzite|23397|5|Briefly described|p463|||Of the McNamara Group.||||||01-FEB-07
19533|Warrina Park Quartzite|23398|5|Briefly described|p454|||Of Mount Isa Group.||||||
19533|Warrina Park Quartzite|23399|4|Described|p493|||Of Mount Isa Group.||||||01-FEB-07
19533|Warrina Park Quartzite|23408|5|Briefly described|p511, p513 Fig. 2, p527|||Of Mount Isa Group.||||||15-JUN-09
19533|Warrina Park Quartzite|23466|5|Briefly described|p273|||Of the Mount Isa Group.||||||01-FEB-07
19533|Warrina Park Quartzite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Mount Isa Group.||||||07-NOV-08
19533|Warrina Park Quartzite|24419|5|Briefly described|p17, p16|Paleoproterozoic|Paleoproterozoic|Basalt unit of Mount Isa Group.  Orthoquartzite, medium-grained flaggy to blocky feldspathic sandstone with abundant ripple marks and cross-bedding, and cross-bedded conglomerate.  Overlies Surprise Creek Formation.  Part of the Prize Supersequence.||||||07-NOV-08
19533|Warrina Park Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group.  Underlies the Moondarra Siltstone.||||||25-AUG-04
19533|Warrina Park Quartzite|30535|2|Defined|p404|Proterozoic|Proterozoic|||||||
19533|Warrina Park Quartzite|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19533|Warrina Park Quartzite|32041|4|Described|p355|||See also p353.||||||01-FEB-07
19533|Warrina Park Quartzite|32660|5|Briefly described|Table 5|||||||||
19533|Warrina Park Quartzite|32959|6|Mentioned|Fig.21|||||||||
19533|Warrina Park Quartzite|33900|4|Described|p13|||||||||
19533|Warrina Park Quartzite|35074|6|Mentioned|Fig.2|||||||||
19533|Warrina Park Quartzite|35114|6|Mentioned|p204|||||||||
19533|Warrina Park Quartzite|35116|6|Mentioned|p177|||||||||
19533|Warrina Park Quartzite|35369|6|Mentioned|Table 1|||Stratigraphy||||||
19533|Warrina Park Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19533|Warrina Park Quartzite|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|38276|6|Mentioned|Fig.1|||||||||
19533|Warrina Park Quartzite|38348|6|Mentioned|p8|||||||||
19533|Warrina Park Quartzite|38350|4|Described|p15|||||||||
19533|Warrina Park Quartzite|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mount Isa group.  Overlain by Moondarra Siltstone.||||||25-AUG-04
19533|Warrina Park Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19533|Warrina Park Quartzite|38834|6|Mentioned|p162|||||||||
19533|Warrina Park Quartzite|38919|6|Mentioned|p496|||||||||
19533|Warrina Park Quartzite|39445|5|Briefly described|Table 2|||See also p35.||||||01-FEB-07
19533|Warrina Park Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mount Isa Group. White medium orthoquartzite, feldspathic quartzite, pebbly sandstone.||||||15-JUN-06
19533|Warrina Park Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
19533|Warrina Park Quartzite|39998|6|Mentioned|p188|||||||||
19533|Warrina Park Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19533|Warrina Park Quartzite|40202|6|Mentioned|p722|||||||||
19533|Warrina Park Quartzite|40221|4|Described|p19|||||||||
19533|Warrina Park Quartzite|40598|6|Mentioned|Fig.2|||||||||
19533|Warrina Park Quartzite|40623|5|Briefly described|p95|||See also p99.||||||01-FEB-07
19533|Warrina Park Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
19533|Warrina Park Quartzite|41307|4|Described|p15|||||||||
19533|Warrina Park Quartzite|45136|4|Described|p49|||||||||
19533|Warrina Park Quartzite|45161|5|Briefly described|Table 8|||||||||
19533|Warrina Park Quartzite|45166|5|Briefly described|p28|||||||||
19533|Warrina Park Quartzite|46801|6|Mentioned|p115|||See also Fig. 14||||||
19533|Warrina Park Quartzite|46960|6|Mentioned|p223|||||||||
19533|Warrina Park Quartzite|47083|5|Briefly described|p18|||Equivalent to Torpedo Creek Quartzite. Of Mount Isa Group. Maximum thickness 100 m.||||||
19533|Warrina Park Quartzite|50100|5|Briefly described|p11, p13 Fig. 4, p19|Statherian|Statherian|Basal unit of Mount Isa Gp.  Comprises orthoquartzite, medium-grained flaggy to blocky feldspathic sandstone with abundant ripple marks and cross-bedding, and cross-bedded conglomerate.  Conformably overlies Surprise Creek Fm.  Geol. Prov: Western Fold Be||||||
19533|Warrina Park Quartzite|50332|4|Described|p16, p20|Paleoproterozoic|Paleoproterozoic|Basal unit of the Mount Isa Group. Conformably underlain by Surprise Creek Formation. Geol Prov: Western Fold Belt Province. Age: ~1700-1640Ma. Consists of  sandstone with abundant ripple marks and cross-bedding, and cross-bedded conglomerate.||||||07-FEB-11
19533|Warrina Park Quartzite|50550|6|Mentioned|p1141 Fig.4||Statherian|Geological Province: Western Fold Belt.||||||19-DEC-07
19533|Warrina Park Quartzite|50624|5|Briefly described|p237 Fig.4||Statherian|Of the Mount Isa Group.||||||01-FEB-07
19533|Warrina Park Quartzite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Meta-arenite and quartzite; minor conglomerate, metasiltstone.||||||
19533|Warrina Park Quartzite|60558|5|Briefly described|p5 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Moondarra Siltstone (Mount Isa Group). Geological Province: Western Fold Belt.||||||03-JUN-09
19533|Warrina Park Quartzite|61923|5|Briefly described|p29 Fig.2, p30, p34 Fig.6|||Of the Mount Isa Group. Comprises two distinct subunits: a mature quartz sandstone with conglomeratic base; and, an orange-weathering, immature, poorly sorted arenite. Conformably overlain by Moondarra Siltstone. Geological Province: Mount Isa Inlier.||||||
19533|Warrina Park Quartzite|62288|5|Briefly described|p122 Fig. 2|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt/ Mount Isa Inlier.||||||07-NOV-08
19533|Warrina Park Quartzite|62535|5|Briefly described|p672|Statherian|Statherian|Leichhardt River Fault Trough.||Mount Isa Group.||||
19533|Warrina Park Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone.||||||30-SEP-08
19533|Warrina Park Quartzite|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Of Gun Supersequence. Age: ~1690+/-7Ma (U/Pb zircon). Geological Province: Isa Superbasin. Conglomeratic and massive quartzite, sandstone, siltstone, claystone, fine-grained feldspathic sandstone, dolomitic sandstone.||||||07-FEB-11
19533|Warrina Park Quartzite|63113|6|Mentioned|p1225 Fig.13. |||Calvert Superbasin. Part of Prize and Gun supersequences.||||||
19533|Warrina Park Quartzite|63114|5|Briefly described|p1253 Fig.2. |||Appears only as Warrina Park. Isa superbasin.||||||
19533|Warrina Park Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Calvert and Isa superbasins.||||||
19533|Warrina Park Quartzite|63116|6|Mentioned|p1297 Fig.2, |||Calvert and Isa superbasins.||||||
19533|Warrina Park Quartzite|63866|5|Briefly described|p58|||||||Overlies the Bigie Formation.||
19533|Warrina Park Quartzite|64250|6|Mentioned|p11 fig 3|||||||Overlies Surprise Creek Formation. Equivalent to Torpedo Creek Quartzite.||
19533|Warrina Park Quartzite|64834|5|Briefly described|p13 Fig.2|||Calvert Superbasin. Western Succession of Mount Isa Basin. Only shown as Warrina Pk in Fig.2.|||||Sandstone.|
19533|Warrina Park Quartzite|65228|6|Mentioned|p23, Fig.04.|||NE of Mount Isa. Basal incision may be a sequence boundary.||||||
19533|Warrina Park Quartzite|65396|6|Mentioned|p82, p175, p241|||Calvert Superbasin. Cover Sequence 2. Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt.||||Overlies Surprise Creek Formation. Equivalent to Torpedo Creek Quartzite.||
19533|Warrina Park Quartzite|66844|5|Briefly described|p265|||Mount Isa region.||Included in Prize Supersequence. Of lower McNamara Group.||Locally overlain by Gun Supersequence sediments.|Sandstone.|
19533|Warrina Park Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Leichhardt River Domain, Mount Isa Inlier. Isa Superbasin. Shown in both Time-Space Plots as Lower and Upper units separated by Carters Bore Rhyolite.|1682 +/- 16 Ma and 1674 +/- 6 Ma (MDA).|Mount Isa Group.|||White medium-grained feldspathic to predominantly quartzose sandstone, pebbly sandstone and minor conglomerate, minor siltstone.|
19533|Warrina Park Quartzite|67499|5|Briefly described|p938, p948|Statherian||Basal unit of the Mount Isa Group. Minimum age determined from SHRIMP zircon dating of the overlying Moondarra Siltstone.|1668 +/- 8 Ma|Of Mount Isa Group||Overlain by the Moondarra Siltstone.|Silicified sandstone and conglomerate.|
19533|Warrina Park Quartzite|68146|6|Mentioned|p199-200|||||||Lateral equivalent to Torpedo Creek Quartzite.||
19533|Warrina Park Quartzite|68542|6|Mentioned|p6|||||||Overlies Surprise Creek Beds, overlain by Moondarra Siltstone||
19533|Warrina Park Quartzite|68575|6|Mentioned|p53|||Mount Isa region.||||||
19533|Warrina Park Quartzite|68576|5|Briefly described|Q_2: p6|||Leichhardt River Fault Trough, Mount Isa Inlier.||Mount Isa Group.||Overlies Surprise Creek Beds. Is overlain by Moondarra Siltstone.||
19533|Warrina Park Quartzite|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Of the Prize Supersequence. Sedimentary depositional ages. See also Warinna Park Quartzite.|1669 +/- 22, 1668+/-8, 1674 +/- 6, 1682 +/- 16 Ma|Mount Isa Group.||||01-DEC-17
19533|Warrina Park Quartzite|69542|6|Mentioned|p133 Fig.2|Mesoproterozoic|Paleoproterozoic|Western Fold Belt.||Mount Isa Group||||
19533|Warrina Park Quartzite|69591|4|Described|p45, p55|||Isa Superbasin. Part of Prize and Gun Supersequences. Fluvial to shallow-marine deposits. This MDA by Neumann et al. (2009) is for the lower part of the unit.|1682 +/- 14 Ma (maximum depositional age).|Basal Mount Isa Group.||Is overlain by Moondarra Siltstone.|White medium-grained feldspathic to predominantly quartzose sandstone, pebbly sandstone and minor conglomerate; minor siltstone.|
19533|Warrina Park Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||White, medium-grained feldspathic to predominantly quartzose sandstone, pebbly sandstone and minor conglomerate; minor siltstone.|
19533|Warrina Park Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Mount Isa Group.|||White, medium-grained feldspathic to predominantly quartzose sandstone, pebbly sandstone and minor conglomerate; minor siltstone.|
19533|Warrina Park Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1674+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite, sandstone.|
19533|Warrina Park Quartzite|71960|4|Described|p85-87, p77, p105, 106|Proterozoic|Proterozoic|In Paroo Range area. High-enery littoral environment. Type section of Derrick et al. (1976) mentioned. Wedges out to west and south. Now called Hero Formation in Hero Fault Zone area.||Of Mount Isa Group.||Lateral equivalent of Hero Formation? Conformably overlain by Moondarra Siltstone. Unconformable in some places over the Surprise Creek Formaiton.|Quartz arenite and well-sorted and rounded conglomerate in Paroo Range.|
19533|Warrina Park Quartzite|71980|5|Briefly described|map legend sheets 1, 2|Proterozoic|Proterozoic|Paroo Range, Western Fault Zone.  Coastal sequences - successive barrier coastline positions.||Of Mount Isa Group|||Coarsening upward felspathic to mainly quartz arenitic sandstone; some beach conglomerate.|
19533|Warrina Park Quartzite|72297|6|Mentioned|p737|||A very pure recrystallised form of this unit is extracted (as lump silica) at the Warrigal mine, E of Mount Isa, for flux in the smelters. Very large resources remain.||||||
19533|Warrina Park Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown, with Torpedo Creek ?Quartzite, as located in the Lawn Hill Platform, Leichhardt River Fault Trough and the Kalkadoon-Leichhardt Belt of the Mount Isa Province and the eastern part of the South Nicholson Basin.||||Overlies Surprise Creek Formation and partially underlies lower Gunpowder Creek Formation and is shown as unconformably underlying Mount Isa Group.||
19533|Warrina Park Quartzite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Leichhardt River Fault Trough, Kalkadoon-Leichhardt Belt and the Lawn Hill Platform of the Mount Isa Province, and the East part of the South Nicholson Basin. U-Pb zircon sedimentary depositional age of overlying 'lower Gunpowder Creek Formation' is 1694+/-3 Ma, and of underlying Surprize Creek Formation is 1688+/-5 Ma.||||Equivalent to Torpedo Creek Quartzite (shown together). Overlies Surprise Creek Formation, shown as partially underlying Gunpowder Creek Formation, lower and unconformably underlying Mount Isa Group.||
19533|Warrina Park Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region and Mount Isa Province, Calvert Superbasin. Listed as Torpedo Creek/Warrina Park Quartzite in Fig.1.2; does not specify / distinguish between the two units.||||Uncertain distinction from Torpedo Creek Quartzite. Underlain by Surprise Creek Formation. Partly overlain by lower Gunpowder Creek Formation.||
19533|Warrina Park Quartzite|73144|6|Mentioned|p10|||Part of the Prize Supersequence.||||||
19533|Warrina Park Quartzite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Leichhardt River Fault Trough.||||||
19533|Warrina Park Quartzite|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Leichhardt River Domain.|1682+/-14 Ma, 1674+/-5 Ma MDA||||Siliciclastics.|
19564|Water Park Creek beds|32357|6|Mentioned|Fig.3|||||||||
19564|Water Park Creek beds|41922|4|Described|Table 1, P8|||||||||
19564|Water Park Creek beds|42660|5|Briefly described|App.3.7 p 199|||||||||
19564|Water Park Creek beds|61035|5|Briefly described|p21|Tertiary|Tertiary|Informal name. Thickness: 500m. Geological Province: Water Park Basin. Consists of carbonaceous shale, sub-bituminous coal, fine to medium-grained sandstone and some oil shale.||||||07-FEB-11
19564|Water Park Creek beds|61155|5|Briefly described|p20|Late Eocene|Middle Eocene|In the Rockhampton-Gladstone area.||||||
19564|Water Park Creek beds|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Oxley and Booval Groups; Petrie, Biloela, Bulimba, Duaringa, Emerald, Exevale, Floraville, Glendower, Louisa, Lowmead, Marion, Red Mountain, Southern Cross, Springvale and Suttor Formations; Beaudesert, Casuarina, Nagoorin, Old Cork, Rossmoya and Takura beds; Fairview Gravel; Moses and Oakdale Sandstones, and unnamed units, are all mapped under the symbol, Tl.||||||
19564|Water Park Creek beds|68679|6|Mentioned|p312-313|Paleogene|Paleogene|Northern New England Orogen.||||||
19564|Water Park Creek beds|69599|5|Briefly described|p586|Eocene|Eocene|Water Park Creek Basin (not spelled out in the text; the LITHOLOGY is similarly inferred). RELATED UNITS (continued): Also correlated (at least partly) with Oakdale Sandstone; Elliott, Petrie, Lowmead Formations.||||Correlated (at least partly) with Beaudesert, Pomona, Fairymead, Takura, Nangorin, Casuarina, Yaamba, Herbert Creek and Rossmoya beds; Flinders Dolomite; see COMMENTS for more.|Shale, carbonaceous shale, coal, sandstone and oil shale.|
19564|Water Park Creek beds|69952|6|Mentioned|p75|Oligocene|Paleocene|||||||
19598|Wathumba beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
19598|Wathumba beach sand|39495|6|Mentioned|p142|||||||||
19598|Wathumba beach sand|62102|5|Briefly described|p367 Tb. 1|||Informal name for morphostratigraphic unit on southeast Queensland coast. Overlapped by Triangle Cliff dune sand.||||||
19600|Watson Creek Volcanics|30914|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19600|Watson Creek Volcanics|35458|6|Mentioned|p239|||Listing of new or revised names of units published recently.||||||
19600|Watson Creek Volcanics|39445|5|Briefly described|Table 7|||||||||
19601|Watsonville Granite|23423|5|Briefly described|p240|||Intrudes Slaughter Yard Creek Volcanics||||||
19601|Watsonville Granite|23506|5|Briefly described|Map Legend||Early Permian|of Ootann Supersuite. Age: ~289+/-16Ma Rb-Sr.||||||
19601|Watsonville Granite|23616|6|Mentioned|Table 1C p44|||||||||
19601|Watsonville Granite|30505|5|Briefly described|p58|||Carboniferous to Permian age||||||
19601|Watsonville Granite|32487|6|Mentioned|p16|||||||||
19601|Watsonville Granite|33205|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19601|Watsonville Granite|39445|6|Mentioned|p90|||Blake 1972.||||||
19601|Watsonville Granite|42547|5|Briefly described|p75|||||||||
19601|Watsonville Granite|43060|5|Briefly described|p100|||||||||
19601|Watsonville Granite|43151|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Of Watsonville Suite (Ootann Supersuite). Pale grey to cream medium-grained to coarse biotite granite; grey, cream or pink , medium- to fine grained biotite granite, locally porphyritic. Age: 289+/-16Ma.||||||15-JUN-06
19601|Watsonville Granite|43259|4|Described|Appendix 1,p33.|Early Permian|Carboniferous|Age is 289+/-16 Ma.||||||
19601|Watsonville Granite|44560|14|Not recorded|p359||Permian|||||||
19601|Watsonville Granite|45065|4|Described|Table 4|||||||||
19601|Watsonville Granite|45113|3|Fully described|p15|||Emphasis on petrography.||||||
19601|Watsonville Granite|46845|6|Mentioned|Table 1|||||||||
19601|Watsonville Granite|46879|6|Mentioned|Fig.1|||||||||
19601|Watsonville Granite|48976|4|Described|p45|||Isotopic data Table 11||||||
19601|Watsonville Granite|60425|4|Described|p45 Tb. 3, p280-1 Appdx. |Middle Permian|Middle Permian|Of Watsonville Suite (Ootann Supersuite). Age: ~281Ma, 289+/-16Ma (Rb-Sr). Cuts the Walsh Bluff Volcanics. I-type.||||||07-FEB-11
19658|Weberra Granite|22438|3|Fully described|p545-547, Fig.12|Statherian|Statherian|Intrudes the uppermost sequences of the Leichhardt Superbasin.||||||19-DEC-06
19658|Weberra Granite|22585|6|Mentioned|Fig1 P736, Fig3||Statherian|||||||
19658|Weberra Granite|22665|6|Mentioned|P230|||||||||
19658|Weberra Granite|23031|5|Briefly described|24|Paleoproterozoic|Paleoproterozoic|Geological province: Mount Isa Fold Belt.||||||07-NOV-08
19658|Weberra Granite|23363|5|Briefly described|344 Fig.3|||||||||
19658|Weberra Granite|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
19658|Weberra Granite|23396|6|Mentioned|p426|||||||||
19658|Weberra Granite|23398|5|Briefly described|p433 Fig.2|Statherian|Statherian|Age: 1698+/-24Ma.||||||19-DEC-06
19658|Weberra Granite|23408|6|Mentioned|p513 Fig. 2|||||||||
19658|Weberra Granite|23466|5|Briefly described|p275|||||||||
19658|Weberra Granite|23545|5|Briefly described|Fig 1 p604|||||||||
19658|Weberra Granite|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin. See also p1955.||||||
19658|Weberra Granite|23776|5|Briefly described|p707 Fig 4|Statherian|Statherian|Age: 1698+/-24 Ma. Of McArthur Group.||||||19-DEC-06
19658|Weberra Granite|24197|5|Briefly described|p28, p95 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Fiery Supersuite. Age: 1678Ma. Geological Province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
19658|Weberra Granite|24307|5|Briefly described|p978|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Block||||||07-NOV-08
19658|Weberra Granite|24308|5|Briefly described|p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Fiery Suite.  Geological Province: Western Fold Belt, Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
19658|Weberra Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
19658|Weberra Granite|32660|5|Briefly described|Table 5|||||||||
19658|Weberra Granite|32959|6|Mentioned|Fig.21|||||||||
19658|Weberra Granite|33387|6|Mentioned|p349|||||||||
19658|Weberra Granite|33900|5|Briefly described|p22|||||||||
19658|Weberra Granite|35074|6|Mentioned|Fig.2|||||||||
19658|Weberra Granite|36548|6|Mentioned|p513|||||||||
19658|Weberra Granite|37459|6|Mentioned|p423|||||||||
19658|Weberra Granite|37462|4|Described|Table4.VII|||||||||
19658|Weberra Granite|37568|6|Mentioned|p83|||||||||
19658|Weberra Granite|38232|6|Mentioned|p89|||||||||
19658|Weberra Granite|38348|6|Mentioned|p6|||||||||
19658|Weberra Granite|39445|5|Briefly described|Table 2|||See also p36 and p40.||||||19-DEC-06
19658|Weberra Granite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Medium to coarse granite, leucogranite, medium graphic granite. May be partly coeval with Fiery Creek Volcanics.||||||15-JUN-06
19658|Weberra Granite|39944|6|Mentioned|p229|||||||||
19658|Weberra Granite|40840|6|Mentioned|Map legend|||||||||
19658|Weberra Granite|41465|6|Mentioned|p12|||||||||
19658|Weberra Granite|41862|6|Mentioned|p474|||||||||
19658|Weberra Granite|41978|6|Mentioned|p502|||||||||
19658|Weberra Granite|41979|4|Described|p522|||||||||
19658|Weberra Granite|42565|5|Briefly described|Table 2 P7|||||||||
19658|Weberra Granite|43010|5|Briefly described|p81|||||||||
19658|Weberra Granite|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|44257|14|Not recorded|p22|||||||||
19658|Weberra Granite|44271|14|Not recorded|p37,38,45,52,53|||Intrudes Ploughed Mountain Beds.||||||
19658|Weberra Granite|44274|14|Not recorded|Tb.2,p13,map||Paleoproterozoic|||||||07-NOV-08
19658|Weberra Granite|44275|14|Not recorded|Map Legend|||||||||
19658|Weberra Granite|44751|14|Not recorded|p30||Precambrian|||||||
19658|Weberra Granite|44989|2|Defined|p.154-6|||Tb.IV. On many pages. Intrudes Ploughed Mountain Beds. (E54-9,13).||||||
19658|Weberra Granite|45166|5|Briefly described|p33|||||||||
19658|Weberra Granite|45287|14|Not recorded|p.229|||||||||
19658|Weberra Granite|46960|6|Mentioned|p216|||||||||
19658|Weberra Granite|47083|4|Described|p21|||Previously included a pluton now mapped as Yeldham Granite. Comagmatic with Fiery Creek Volcanics. Intrudes Quilalar Formation and Myally Subgroup. A-type granite.||||||29-APR-16
19658|Weberra Granite|49041|5|Briefly described|Table 1|||Mention Table 4||||||
19658|Weberra Granite|50536|5|Briefly described|p1.4, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Fiery Suite. Age: 1678-1698 +/- 24Ma (U-Pb).||||||07-NOV-08
19658|Weberra Granite|61929|5|Briefly described|p128 Fig. 2|||||||||
19658|Weberra Granite|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: ca1700Ma. See also p192 Fig. 5.||||||07-NOV-08
19658|Weberra Granite|62988|5|Briefly described|p34|Paleoproterozoic|Paleoproterozoic|Part of the ~1710Ma Fiery Event, together with Fiery Creek Volcanics. Geological Province: Mount Isa Inlier.||||||07-NOV-08
19658|Weberra Granite|63023|5|Briefly described|p1035|Paleoproterozoic|Paleoproterozoic|Age: ca 1700Ma. Geological Province: Western Fold Belt.||||||07-NOV-08
19658|Weberra Granite|63109|6|Mentioned|p1109|||Age: ~1710Ma (Hone et al., 1987).||||||
19658|Weberra Granite|63110|6|Mentioned|p1141 Fig. 17|Statherian|Statherian|Geological Province: Calvert Superbasin.||||||11-JUN-08
19658|Weberra Granite|63866|5|Briefly described|p57|Statherian|Statherian|Calvert Superbasin.|1711 +/-3 Ma (Neumann et al., 2006)|||||
19658|Weberra Granite|64250|6|Mentioned|p11 fig 3, p19, p21, p24|||Western Fold Belt, Mount Isa Inlier. Co-magmatic with Fiery Creek Volcanics.|1711 +/- 3 Ma|||||
19658|Weberra Granite|65228|5|Briefly described|Figs.04, 10.|Statherian|Statherian|Mount Isa area. Mis-spelt as Webbera in Fig.10. Poor time constraint. Probably coeval with Fiery Creek Volcanics (1709 +/- 3 Ma).|1698 +/- 24 Ma.|||||
19658|Weberra Granite|65396|6|Mentioned|p82, p175, p187, p193, p197, p241|Statherian|Statherian|Calvert Superbasin. Cover Sequence 2. Co-magmatic with 1709 +/- 3 Ma Fiery Creek Volcanics.|1698 +/- 24 Ma|||||
19658|Weberra Granite|66844|6|Mentioned|p245|Statherian|Statherian|Isa Superbasin. Age from SHRIMP dating.|1695+\-24 Ma|||||
19658|Weberra Granite|67323|5|Briefly described|GIS attrib tbl, p11, p24, p33, p41, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Weberra Igneous Event; initiation of Calvert Superbasin. Mount Oxide Domain, Mount Isa Inlier. Forms core of the Fiery Creek Dome. Included in a list of Suites on p41.|1711+/-3 Ma (Neumann et al. 2009).|||Coeval with Fiery Creek Volcanics.|Medium to coarse granite, leucogranite, medium graphic granite.|
19658|Weberra Granite|68021|5|Briefly described|p135 fig 4, p136|Statherian|Statherian||1710 Ma|||Intrudes Bigie Formation and possibly Quilalar Formation.||
19658|Weberra Granite|68542|6|Mentioned|p1 |||||||||
19658|Weberra Granite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
19658|Weberra Granite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
19658|Weberra Granite|68732|5|Briefly described|p165 Fig.3|Statherian|Statherian|Of the Big Supersequence. Igneous crystallisation age. Age assumed to be determined with SHRIMP.|1711 +/- 3 Ma|||||04-APR-18
19658|Weberra Granite|69222|6|Mentioned|p222 Fig.2, p225 Tb.2|Statherian|Statherian|Heat flow values given.|1698 +/- 24 Ma (Wyborn et al., 1998).|||||09-FEB-18
19658|Weberra Granite|69370|6|Mentioned|p307 Fig.2|Statherian|Statherian|Western Fold Belt, Mount Isa Block.||||Intrudes Surprise Creek Formation.||25-JAN-19
19658|Weberra Granite|69591|5|Briefly described|p28, p37-39, p59, p106|Paleoproterozoic|Paleoproterozoic|Mount Oxide Domain, Calvert Superbasin. Syn-extensional. Forms the northern exposure of a NE-trending belt of laccoliths in the footwall of the Fiery Creek Fault Zone. Coeval with the Fiery Creek Volcanics. Wyborn et al. (1998) dated this unit at 1698 +/- 28 Ma.|1710 Ma.||||Medium to coarse granite, leucogranite, medium graphic granite.|
19658|Weberra Granite|70858|6|Mentioned|p31|Paleoproterozoic|Paleoproterozoic|Calvert Superbasin.|1710 Ma.|||||
19658|Weberra Granite|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1711+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
19658|Weberra Granite|71799|5|Briefly described|p154|Statherian|Statherian|Lawn Hill Platform.|1711 +/- 3 Ma (Neumann et al, 2006)|||||
19658|Weberra Granite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin. Age given as U-Pb zircon igneous crystallisation age.|1711 +/-3 Ma|||||
19658|Weberra Granite|72889|6|Mentioned|p6 Fig.i.|||||||||
19658|Weberra Granite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|U-Pb zircon igneous crystallisation age (Ma) shown.|1711 +/- 3 Ma|||Shown as younger than Carrara Range Group.||
19658|Weberra Granite|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Calvert Superbasin. Geochronology is a U-Pb zircon igneous crystallisation age.|1711 +/- 3 Ma (see Fig.1.2)|||Partly overlain(?) by Surprise Creek Formation unconformably.||
19658|Weberra Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform. [Written as Weberra Granitte].||||||
19691|Weir Basalt|29386|6|Mentioned|p454|||Upper Triassic.||||||
19691|Weir Basalt|30302|6|Mentioned|p414|||Refers Allen(1959)||||||
19691|Weir Basalt|30465|6|Mentioned|p3|||||||||
19691|Weir Basalt|32180|5|Briefly described|p4|||||||||
19691|Weir Basalt|33381|4|Described|p112|||Triassic. See also P117||||||
19691|Weir Basalt|35161|6|Mentioned|p591|||||||||
19691|Weir Basalt|36779|6|Mentioned|p6|||||||||
19691|Weir Basalt|37111|5|Briefly described|p292|||||||||
19691|Weir Basalt|38074|5|Briefly described|Table 1|||||||||
19691|Weir Basalt|38076|6|Mentioned|Table 3|||||||||
19691|Weir Basalt|38307|6|Mentioned|Fig.1|||||||||
19691|Weir Basalt|38441|6|Mentioned|Map legend|Carnian|Carnian|||||||
19691|Weir Basalt|39445|6|Mentioned|Table 9|||||||||
19691|Weir Basalt|40623|5|Briefly described|p30|||Mention Table 2||||||
19691|Weir Basalt|41906|3|Fully described|Table 2 P19|||||||||
19691|Weir Basalt|42336|5|Briefly described|Table 1 P5|||||||||
19691|Weir Basalt|43076|6|Mentioned|p5|||||||||
19691|Weir Basalt|43150|5|Briefly described|Map Legend||Triassic|Of the Ipswich Coal Measures. Geological Province: Ipswich Basin.||||||12-APR-05
19691|Weir Basalt|43922|14|Not recorded|p324,325|||Formation of Kholo Subgroup of Ipswich Coal Measures (basal unit).||||||
19691|Weir Basalt|44026|14|Not recorded|p122||Triassic|Lithological equivalent of Neara Volcanics.||||||
19691|Weir Basalt|44510|2|Defined|p252-253,Fig.35|||Overlies unconformably on Neranleigh-Fernvale Group. Equivalent to Sugars Basalt.||||||
19691|Weir Basalt|44542|2|Defined|p32,33||Middle Triassic|Overlain by Blackwall Breccia.||||||
19691|Weir Basalt|44705|14|Not recorded|p1-4,6-7,10,15,16|||||||||
19691|Weir Basalt|44707|14|Not recorded|p3|||||||||
19691|Weir Basalt|44775|14|Not recorded|p7,8,map 2||Triassic|||||||
19691|Weir Basalt|44783|14|Not recorded|p16,18|||||||||
19691|Weir Basalt|44786|14|Not recorded|p193-202|||||||||
19691|Weir Basalt|45087|5|Briefly described|p154|||Chemical analyses||||||
19691|Weir Basalt|67402|6|Mentioned|p222, p223|||||||Overlies the Blackwall Breccia.|Sub-aerial basalt.|
19691|Weir Basalt|68679|5|Briefly described|p393-394, p435|Late Triassic|Late Triassic|Ipswich Basin. 11m thick in the type section; up to 30m thick in drill holes.||Kholo Subgroup.||Overlies and interfingers with Blackwall Breccia; unconformably overlies Neranleigh-Fernvale beds. Is overlain by Mount Crosby Formation. Equivalent to upper Sugars Basalt.|At least four lava flows: basalt to basaltic andesite lavas from aphyric to moderately porphyritic, and from massive to highly amygdaloidal.|
19691|Weir Basalt|73306|6|Mentioned|p565-566|Late Triassic|Late Triassic|Ipswich Basin.||||||
19714|Wellington Springs Tonalite|22847|3|Fully described|p 54|Early Devonian|Late Silurian|||||||
19714|Wellington Springs Tonalite|42633|6|Mentioned|Table 1 P8|||NOT reserved.||||||
19714|Wellington Springs Tonalite|43093|4|Described|Appendix 1|Early Devonian|Late Silurian|||||||
19714|Wellington Springs Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Wellington Springs ton.||Unit in Millchester Supersuite.||||
19733|Wenlock Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Fluvial deposits.  Of the Garroway Sandstone.||||||
19733|Wenlock Member|32705|6|Mentioned|p179|||||||||
19733|Wenlock Member|42061|5|Briefly described|Fig.4 P151|||||||||
19733|Wenlock Member|62837|5|Briefly described|Stratigraphic columns|Bathonian|Bathonian|Of the Garraway Formation. Age: 170-~163Ma. Geological Province: Northern Cape York.||||||01-MAR-10
19776|West Boorama Granite|42556|5|Briefly described|Fig.2 P4|||||||||
19779|West Branch Creek beds|42216|5|Briefly described|p425|||See also Fig.1||||||
19796|Westbourne Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499, p501|Kimmeridgian|Oxfordian|Northern Surat and eastern Eromanga Basins. Thickness generally 80-100m, up to 200m.||Unit in Injune Creek Group.||Conformably overlies Adori Sandstone. Interfingers with Pilliga Sandstone and lower Kumbarilla beds.|Cross-bedded, quartzose to sub-labile sandstone, siltstone and mudstone with lenticular bentonite beds and thin coal seams.|
19796|Westbourne Formation|13497|6|Mentioned|p115 fig 6.33, p130|Late Jurassic|Late Jurassic|Eromanga Basin. See also p141, p144 fig 9.2, p146, p148-p154, p216.||||Overlies the Adori Sandstone. Interfingers with and is overlain by the Namur Sandstone.||
19796|Westbourne Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Jurassic|Late Jurassic|In Eromanga Basin.||||||
19796|Westbourne Formation|22464|6|Mentioned|p9||Late Jurassic|Eromanga Basin. Overlies Adori Sandstone||||||
19796|Westbourne Formation|22857|5|Briefly described|p296-7 Tb.22.1, p314-5|Tithonian|Callovian|Fine-grained sandstone interbedded with siltstone, claystone, minor coal. Max. thickness: 220m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
19796|Westbourne Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Callovian|||||||
19796|Westbourne Formation|22883|6|Mentioned|P31|||||||||
19796|Westbourne Formation|23054|6|Mentioned|Fig5p22|Berriasian|Tithonian|||||||
19796|Westbourne Formation|23056|4|Described|20|||Geol province Eromanga Basin. Of the Injune Creek Group. Underlain by Adori Sandstone.||||||17-JAN-08
19796|Westbourne Formation|23155|5|Briefly described|p26|||The Westbourne Formation has not been recognised on STRZELECKI.||||||
19796|Westbourne Formation|23375|4|Described|Fig2 p265, 291|Tithonian|Tithonian|Laterally equivalent to part of Namur Sandstone. In the Eromanga Basin.||||||17-JAN-08
19796|Westbourne Formation|23425|5|Briefly described|Plate 10.2|||Of Injune Creek Group. Eromanga Basin Province.||||||
19796|Westbourne Formation|23426|5|Briefly described|p403|||Eromanga Basin Province.||||||
19796|Westbourne Formation|23430|4|Described|p523 + p524 Table 14.7|||Of Injune Creek Group. Overlain by Hooray Sandstone - unconformable. Eromanga Basin Province.||||||17-JAN-08
19796|Westbourne Formation|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|23883|5|Briefly described|p129 Fig. 11.2|Late Jurassic|Late Jurassic|Of the Injune Creek Group.  Geological Province: Great Australian Superbasin.||||||
19796|Westbourne Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Of Injune Creek Group. Geological Province: Great Artesian Basin.||||||
19796|Westbourne Formation|24068|4|Described|p270 Table 2|Late Jurassic|Late Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 130m.||||||
19796|Westbourne Formation|24092|5|Briefly described|p8 Fig.3|||Of Injune Creek Group. Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|29591|6|Mentioned|Table 15|||||||||
19796|Westbourne Formation|30021|6|Mentioned|p90|||||||||
19796|Westbourne Formation|30024|6|Mentioned|p332|||||||||
19796|Westbourne Formation|30102|5|Briefly described|p24|||Unit of the Injune Creek Group. See also P21,25,31,34.||||||
19796|Westbourne Formation|30103|5|Briefly described|p9|||Table 3 on P9. Upper Jurassic age.||||||
19796|Westbourne Formation|30104|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
19796|Westbourne Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19796|Westbourne Formation|30691|4|Described|p15|||See also Table 4. Upper Jurassic age||||||
19796|Westbourne Formation|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|30695|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30699|6|Mentioned|p56|||Map||||||
19796|Westbourne Formation|30700|6|Mentioned|p27|||||||||
19796|Westbourne Formation|30702|6|Mentioned|Fig.1|||See also Table 1. Stratigraphic table||||||
19796|Westbourne Formation|30804|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|30853|5|Briefly described|Table 3|||Upper Jurassic age||||||
19796|Westbourne Formation|30854|4|Described|Table 4|||Upper Jurassic age||||||
19796|Westbourne Formation|30855|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Unit in Injune Creek Group||||||
19796|Westbourne Formation|30856|4|Described|Table 3|||On p10. Upper Jurassic age.||||||17-JAN-08
19796|Westbourne Formation|30857|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Part of Injune Creek Group||||||
19796|Westbourne Formation|31116|4|Described|p36|||See also p27.||||||17-JAN-08
19796|Westbourne Formation|31120|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|31145|5|Briefly described|Table 1|||U. Jurassic||||||
19796|Westbourne Formation|31425|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|31431|5|Briefly described|Table 3|||M.-U.Jurassic||||||
19796|Westbourne Formation|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|32138|6|Mentioned|p396|||||||||
19796|Westbourne Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33067|4|Described|Table 1|Late Jurassic|Jurassic|Of the Injune Creek Group.  Siltstone, shale, quartz sandstone.||||||07-JUL-04
19796|Westbourne Formation|33069|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|33071|5|Briefly described|p6|||M.-U.Jur.||||||
19796|Westbourne Formation|33075|6|Mentioned|p445|||||||||
19796|Westbourne Formation|33078|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33079|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33082|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33087|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33088|4|Described|Table 3|||U.Jur.||||||
19796|Westbourne Formation|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
19796|Westbourne Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
19796|Westbourne Formation|33176|6|Mentioned|p175|||Correlated with Loth Fm.||||||
19796|Westbourne Formation|33183|6|Mentioned|p233|||||||||
19796|Westbourne Formation|33367|3|Fully described|p26|||||||||
19796|Westbourne Formation|33371|2|Defined|p58|Jurassic|Jurassic|See also p59. Prob. Jurassic.||||||17-JAN-08
19796|Westbourne Formation|33449|4|Described|Table 1|||U.Jur.||||||
19796|Westbourne Formation|33638|5|Briefly described|Table 1|||||||||
19796|Westbourne Formation|33639|5|Briefly described|Table 2|||||||||
19796|Westbourne Formation|33640|4|Described|Table 3|||M.-U.Jur.||||||
19796|Westbourne Formation|33643|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
19796|Westbourne Formation|33672|5|Briefly described|p44|||Lithology.||||||
19796|Westbourne Formation|33673|4|Described|p291|||See also p287||||||17-JAN-08
19796|Westbourne Formation|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33825|5|Briefly described|p9,10|||Equiv. correl. Lithology. Correlation table.||||||
19796|Westbourne Formation|33827|6|Mentioned|p13|||||||||
19796|Westbourne Formation|33939|6|Mentioned|p412|||||||||
19796|Westbourne Formation|33998|6|Mentioned|p31|||||||||
19796|Westbourne Formation|34065|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|34091|5|Briefly described|Table 1|||Jur.||||||
19796|Westbourne Formation|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
19796|Westbourne Formation|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34218|4|Described|Table 1|||Upper Jurassic. See also Table 2.||||||
19796|Westbourne Formation|34386|6|Mentioned|p97|||Jurassic. See also P98,99,100 etc.||||||
19796|Westbourne Formation|34486|4|Described|Table 1|||See also Table 2, p10. Upper Jurassic.||||||17-JAN-08
19796|Westbourne Formation|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19796|Westbourne Formation|35239|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|35560|6|Mentioned|p289|||||||||
19796|Westbourne Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
19796|Westbourne Formation|35663|5|Briefly described|p126|||||||||
19796|Westbourne Formation|35811|5|Briefly described|Table 3|||||||||
19796|Westbourne Formation|35937|6|Mentioned|Fig.5|||||||||
19796|Westbourne Formation|36243|6|Mentioned|Table 6A|||||||||
19796|Westbourne Formation|36251|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|36570|6|Mentioned|p55|||||||||
19796|Westbourne Formation|36910|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|37117|5|Briefly described|p313|||||||||
19796|Westbourne Formation|37287|6|Mentioned|p36|||||||||
19796|Westbourne Formation|37608|3|Fully described|Table 1|||||||||
19796|Westbourne Formation|37995|4|Described|p64|||||||||
19796|Westbourne Formation|38199|6|Mentioned|p423|||||||||
19796|Westbourne Formation|38226|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|38779|6|Mentioned|p7|||||||||
19796|Westbourne Formation|39070|4|Described|p363|||||||||
19796|Westbourne Formation|39212|5|Briefly described|p16|||See also P38||||||
19796|Westbourne Formation|39276|6|Mentioned|Fig. 2|||||||||
19796|Westbourne Formation|39445|5|Briefly described|Table 10|||||||||
19796|Westbourne Formation|39478|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|39494|6|Mentioned|p129|||See also Figs 3,5||||||
19796|Westbourne Formation|39846|6|Mentioned|p45|||||||||
19796|Westbourne Formation|39847|5|Briefly described|p36|||||||||
19796|Westbourne Formation|39914|6|Mentioned|p2|||||||||
19796|Westbourne Formation|39943|6|Mentioned|Table 8A|||||||||
19796|Westbourne Formation|39988|6|Mentioned|p289|||||||||
19796|Westbourne Formation|39989|4|Described|p422|||||||||
19796|Westbourne Formation|40030|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|40121|6|Mentioned|p446|||||||||
19796|Westbourne Formation|40199|6|Mentioned|Fig.1|||||||||
19796|Westbourne Formation|40245|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40249|6|Mentioned|p38|||Mention P41||||||
19796|Westbourne Formation|40250|6|Mentioned|Fig.7|||||||||
19796|Westbourne Formation|40540|6|Mentioned|p155|||||||||
19796|Westbourne Formation|40541|3|Fully described|p110|||||||||
19796|Westbourne Formation|40544|6|Mentioned|p159|||See also Fig.6||||||
19796|Westbourne Formation|40666|4|Described|p357|||||||||
19796|Westbourne Formation|40670|6|Mentioned|Fig.9|||||||||
19796|Westbourne Formation|40675|6|Mentioned|Table 8A|||Mention Table 9A||||||
19796|Westbourne Formation|40687|3|Fully described|p416|||||||||
19796|Westbourne Formation|40832|3|Fully described|p456|||||||||
19796|Westbourne Formation|40833|6|Mentioned|p468|||||||||
19796|Westbourne Formation|40910|6|Mentioned|Table 3|||||||||
19796|Westbourne Formation|40926|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40962|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41060|6|Mentioned|p7|||Generalized stratigraphy||||||
19796|Westbourne Formation|41061|6|Mentioned|p19|||||||||
19796|Westbourne Formation|41062|6|Mentioned|p27|||See also P34 and Fig.5||||||
19796|Westbourne Formation|41063|6|Mentioned|p40|||||||||
19796|Westbourne Formation|41064|6|Mentioned|p60|||||||||
19796|Westbourne Formation|41084|5|Briefly described|p80|||See also Fig.2||||||
19796|Westbourne Formation|41097|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41099|6|Mentioned|p192|||||||||
19796|Westbourne Formation|41123|6|Mentioned|p177|||||||||
19796|Westbourne Formation|41175|5|Briefly described|p195|||||||||
19796|Westbourne Formation|41176|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|41177|6|Mentioned|p222|||||||||
19796|Westbourne Formation|41182|5|Briefly described|Fig.2|||||||||
19796|Westbourne Formation|41183|6|Mentioned|p310|||||||||
19796|Westbourne Formation|41186|4|Described|p208|||||||||
19796|Westbourne Formation|41187|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|41198|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41210|5|Briefly described|Fig.3|||||||||
19796|Westbourne Formation|41214|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41216|6|Mentioned|p300|||See also Fig.18||||||
19796|Westbourne Formation|41219|4|Described|p346|||||||||
19796|Westbourne Formation|41247|6|Mentioned|p120|||||||||
19796|Westbourne Formation|41266|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41681|6|Mentioned|p10|||See also P13||||||
19796|Westbourne Formation|41707|5|Briefly described|p163|||||||||
19796|Westbourne Formation|41724|6|Mentioned|p382|||||||||
19796|Westbourne Formation|41992|4|Described|Fig.2 P183|||||||||
19796|Westbourne Formation|42007|5|Briefly described|Fig.2 P182|||||||||
19796|Westbourne Formation|42061|4|Described|Fig,11 P159|||||||||
19796|Westbourne Formation|42067|4|Described|p308|||See also appendix 2||||||
19796|Westbourne Formation|42071|6|Mentioned|p117|||||||||
19796|Westbourne Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19796|Westbourne Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19796|Westbourne Formation|42397|5|Briefly described|p10|||||||||
19796|Westbourne Formation|42446|4|Described|p12|||||||||
19796|Westbourne Formation|42447|5|Briefly described|p5 + Fig. 1|||||||||
19796|Westbourne Formation|42463|6|Mentioned|Fig.5 P172|||||||||
19796|Westbourne Formation|42474|6|Mentioned|p25|||||||||
19796|Westbourne Formation|42493|5|Briefly described|p20, Fig.1 p18|||||||||
19796|Westbourne Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19796|Westbourne Formation|42520|5|Briefly described|p6|||||||||
19796|Westbourne Formation|42634|6|Mentioned|p12|||||||||
19796|Westbourne Formation|42746|5|Briefly described|p9, p10|||See also Fig.6 P8, Fig.7 P37||||||
19796|Westbourne Formation|42749|4|Described|p30, Fig.5 p29|||see also Fig.2 p27.||||||17-JAN-08
19796|Westbourne Formation|42999|5|Briefly described|Table 2,p90||Late Jurassic|||||||
19796|Westbourne Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
19796|Westbourne Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19796|Westbourne Formation|43004|5|Briefly described|Table 1,p179|||||||||
19796|Westbourne Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19796|Westbourne Formation|43114|5|Briefly described|p12|||||||||
19796|Westbourne Formation|43122|5|Briefly described|p11|||see also Fig. 2.||||||
19796|Westbourne Formation|43404|14|Not recorded|Table p11||Late Jurassic|||||||
19796|Westbourne Formation|43591|6|Mentioned|p40|||||||||
19796|Westbourne Formation|43628|6|Mentioned|Fig.13||Late Jurassic|||||||
19796|Westbourne Formation|43711|6|Mentioned|p18|||||||||
19796|Westbourne Formation|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
19796|Westbourne Formation|44016|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44019|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44020|14|Not recorded|Tb.1,2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
19796|Westbourne Formation|44021|14|Not recorded|p232-234,236-238||Late Jurassic|="Upper Intermediate Series" of Woolley 1941. Is upper part of Injune Creek Group. Overlies Birkhead Formation. Overlain by "Hooray Sandstone". Overlies Adori Sandstone. Plants and spores.||||||
19796|Westbourne Formation|44022|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44023|4|Described|Tb.3,p12||Late Jurassic|||||||
19796|Westbourne Formation|44027|14|Not recorded|p110||Late Jurassic|||||||
19796|Westbourne Formation|44028|14|Not recorded|Fig.2,7,p514||Jurassic|Of Injune Creek Group. See Strat Table.||||||
19796|Westbourne Formation|44031|14|Not recorded|p5,8,12,13||Jurassic|||||||
19796|Westbourne Formation|44084|14|Not recorded|p32(Tb)|||||||||
19796|Westbourne Formation|44133|5|Briefly described|p110, 104 Fig. 9.11|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin. Conformably overlies: Adori Sandstone. Overlain and intertongued by Namur Sandstone.||||||28-SEP-16
19796|Westbourne Formation|44171|14|Not recorded|p194,19,197,198|||||||||
19796|Westbourne Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
19796|Westbourne Formation|44374|14|Not recorded|p11|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44414|14|Not recorded|p112-115|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44415|14|Not recorded|Fig.2,p23|||||||||
19796|Westbourne Formation|45071|3|Fully described|Table 15|||See also p82.||||||17-JAN-08
19796|Westbourne Formation|45110|2|Defined|p97|Late Jurassic|Late Jurassic|See also Fig.5 and p24.||||||17-JAN-08
19796|Westbourne Formation|46791|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19796|Westbourne Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19796|Westbourne Formation|46984|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|48919|4|Described|p63|||U.Jurassic. See also p64-65.||||||17-JAN-08
19796|Westbourne Formation|48920|3|Fully described|p53|||Part of Injune Creek Group.||||||16-SEP-08
19796|Westbourne Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19796|Westbourne Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19796|Westbourne Formation|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Adori Sandstone; overlain by Murta Formation; lateral to Adori Sandstone? Geological Province: Eromanga  Basin.||||||31-JAN-08
19796|Westbourne Formation|60993|5|Briefly described|p36|||Of the Injune Creek Group. May be the equivalent of the upper sandstone section of the Woodenbong beds. Geological Province: Surat Basin.||||||
19796|Westbourne Formation|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61000|5|Briefly described|p186 Fig. 4|Tithonian|Callovian|Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61312|5|Briefly described|p67 Fig. E5|Late Jurassic|Jurassic|Of the Injune Creek Group. Siltstone, shale and fine-grained quartzose sandstone; productive reservoir unit. Geological Province: Eromanga Basin. See also p79 Table E2.||||||
19796|Westbourne Formation|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Jurassic|Shale, siltstone, quartz sandstone, minor coal. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
19796|Westbourne Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19796|Westbourne Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61614|6|Mentioned|p290 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
19796|Westbourne Formation|61615|6|Mentioned|p302 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61823|5|Briefly described|p118|Cretaceous|Jurassic|Fluvial-lacustrine sediments. Geological Province:  Eromanga Basin.||||||
19796|Westbourne Formation|62730|5|Briefly described|p352 Fig. 1|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
19796|Westbourne Formation|63218|6|Mentioned|p211 Fig.2. |Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.|Includes Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|63979|4|Described|p38-39, Fig. 44|Tithonian|Oxford|Conformable on Adori Sst; overlain by/intertongues with Hooray Sst. and "upper Namur Sst". Max.thickness:166m. Fine to v.fine, rarely med.- to coarse-gr. sst, moderately to poorly sorted, interlaminated/interbedded with siltst.+ shale. In Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses some hydrocarbon source potential.||||||07-FEB-11
19796|Westbourne Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Jurassic|Late Jurassic|Eromanga and Surat/Bowen Basins.||||Eromanga Basin: overlies Adori Sandstone; underlies Hooray Sandstone. Surat/Bowen Basins: overlies Springbok Sandstone; underlies Gubberamunda Sandstone.||11-DEC-15
19796|Westbourne Formation|64665|5|Briefly described|p53 Fig.2, p60.|Late Jurassic|Late Jurassic|Eromanga and Surat Basins. Contains thin coals.||Upper unit in Injune Creek Group.||Overlies Adori and Springbok Sandstones.||
19796|Westbourne Formation|64856|3|Fully described|p79, p88-95|Tithonian|Oxfordian|Defined by American Overseas Petroleum Ltd (1964) with a type section 389-503m in AOP Westbourne 1 well. Eromanga and Surat Basins. Interbedded shales and siltstones and very fine-grained, quartzose sandstones. Includes Norwood Mudstone Member. Conformably overlies the Springbok Sandstone, intertongues and grades into the Pilliga Sandstone to south. Underlies Gubberamunda Sandstone. Up to 220m thick. Age from palynoflora (units APJ5, 6).||||||18-JAN-22
19796|Westbourne Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Springbok Sandstone, Surat Basin.||||||
19796|Westbourne Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19796|Westbourne Formation|65003|5|Briefly described|p8||Jurassic|Of Surat Basin.||||||
19796|Westbourne Formation|65112|5|Briefly described|p323; p328; Fig 11 p 324; fig 16 p328|Jurassic|Jurassic||156-142 Ma.|||Overlies Springbok Sandstone, underlies Gubberamunda Sandstone.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
19796|Westbourne Formation|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Late Jurassic|Overlies the Springbok Formation, underlies Gubberamunda Sandstone.||||||
19796|Westbourne Formation|65114|5|Briefly described|p385 Fig.3|Late Jurassic||||||||
19796|Westbourne Formation|65116|5|Briefly described|Fig 2 p437|Late Jurassic|Late Jurassic|Underlies the Gubberamunda Sandstone, overlies the Springbok Sandstone, Surat Basin.||||||06-MAR-12
19796|Westbourne Formation|65117|5|Briefly described|p463, 471-472,  474,  Fig 4 p465|Tithonian|Oxfordian|Surat Basin, up to 200m thick. Conformable on Springbok Sandstone. Diachronous base. Older in Surat than Eromanga Basins. Interbedded mudstone, siltstone, coal and very fine grained quartzose to lithic-feldspathic sandstone.||||||
19796|Westbourne Formation|65119|6|Mentioned|Fig 6 p512, Fig 13-14|||Present in the Cabawin 1 and Rockwood 1 wells.||||||07-MAR-12
19796|Westbourne Formation|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Overbank and lacustrine-swamp deposits.||||||
19796|Westbourne Formation|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Late Jurassic|Of Eromanga Basin. Overlies Adori Sandstone. Sediment with volcanic component. See also "uppermost Westbourne Formation".||||||08-MAR-12
19796|Westbourne Formation|65489|5|Briefly described|p15, p49, p96, p155|Late Jurassic|Late Jurassic|Eromanga Basin. 210m thick. Fair source rock. Potential for stratigraphic structural traps. Oil reservoir accounting for 4% of the Basin's production.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||Unit in Injune Creek Group.||Overlies Adori or Springbok Sandstones. Is overlain by Namur, Hooray or Gubberamunda Sandstones.||
19796|Westbourne Formation|66623|6|Mentioned|p239.|Early Cretaceous|Late Jurassic|||||||
19796|Westbourne Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga and Surat Basins. In Fig.3 also shows "uppermost Westbourne Formation" in Eromanga Basin.||Injune Creek Group||||
19796|Westbourne Formation|67133|5|Briefly described|p2, p5, p15-16, p18-21|Jurassic|Jurassic|32 samples of this unit were analysed by XRD and optical microscopy for this study. Deposited in a lacustrine delta environment. Quartz is the main component (18-80%) with feldspars (12-40%); plagioclase is always dominant. Kaolinite (up to 33%) is the dominant clay mineral. The mixed-layer clays are highly variable.||||Conformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.|Very fine- to medium-grained, fairly to poorly sorted, sublabile to quartzose, often massive sandstones with laminated to thinly-bedded siltstones and shales.|
19796|Westbourne Formation|67323|5|Briefly described|p87-88, p93, p95 Fig.12.5|Late Jurassic|Late Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin.||||Overlies Adori Sandstone. Is overlain by Hooray Sandstone.||
19796|Westbourne Formation|67402|4|Described|p26, p26 tbl RRM4, p108|Berriasian|Oxfordian|Eromanga Basin. Potential conventional seal for the storage of carbon dioxide. Proven seal of the Springbok Formation. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Maximum thickness of 160m. Demonstrated hydrocarbon seal. See also p109, p113, p115, p123, p146, p148, p151, p152, p154 fig SRT15/16, p156, p226, p265.||||Overlies the Adori Sandstone. Conformably overlies the Springbok Sandstone. Overlain by the Hooray Sandstone.|Fine to very fine-grained sandstone, interlaminated and interbedded with siltstone and shale.|
19796|Westbourne Formation|67561|5|Briefly described|p52 Fig.2, p58 Fig.7, p59 Fig.8|Valanginian|Berriasian|Australian Spore-Pollen zonation: C.watherooensis.||||||
19796|Westbourne Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68117|5|Briefly described|p345-346|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.|Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|68135|5|Briefly described|p52 fig 2b, p57 fig 4|Tithonian|Kimmeridgian|Surat Basin (QLD) and Eromanga Basin.||||Overlies Springbok and Adori Sandstones. Is unconformably overlain by Gubberamunda, Hooray and Namur Sandstones.|Interbedded sandstone and siltstone.|15-SEP-17
19796|Westbourne Formation|68139|6|Mentioned|p23|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19796|Westbourne Formation|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Overlies Springbok Sandstone. Is overlain unconformably by Gubberamunda Sandstone.||
19796|Westbourne Formation|68731|6|Mentioned|pp209-211|||||||||
19796|Westbourne Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
19796|Westbourne Formation|69019|5|Briefly described|p85 Fig.21.|Berriasian|Tithonian|Southern Eromanga Basin.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|69023|6|Mentioned|p89 Fig.20, p91|Berriasian|Tithonian|||||Intertongues with lower part of Namur Sandstone.||
19796|Westbourne Formation|69457|6|Mentioned|p41:3-4|||Eromanga Basin.||||||12-JUL-16
19796|Westbourne Formation|69582|5|Briefly described|p36, p38, p65-p66|Late Jurassic|Late Jurassic|Eromanga Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Springbok Sandstone and the Adori Sandstone. Unconformably overlain by the Gubberamunda Sandstone. Overlain by the Hooray Sandstone.|Mudstone, sandstone, siltstone.|
19796|Westbourne Formation|69594|3|Fully described|p519, p525-527, p531, p537, p573|Tithonian|Kimmeridgian|Exon (1966). Swarbrick et al. (1973) defined the lower part as the Norwood Mudstone Member. Eromanga, northern Surat Basins. The type section is 390-503m in AOP Westbourne 1, near Tambo. Discrimination from Adori Sandstone described. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated. Up to 250m thick. Basal fluviatile, later lacustrine deposits. Has hydrocarbon source potential; is a significant reservoir. RELATED UNITS (continued): Is overlain by and interfingers with both Namur and Hooray Sandstones; is overlain conformably to unconformably by the upper Namur Sandstone; and Gubberamunda Sandstone conformably (locally disconformably).||Injune Creek Group.|Norwood Mudstone Member.|Conformably overlies Adori and Springbok Sandstones. Interdigitates with and passes into Pilliga Sandstone. See COMMENTS for more.|Fine, very fine, rarely medium or coarse, labile micaceous sandstones with interbedded siltstone and shale.|
19796|Westbourne Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Jurassic|||||Overlies Adori Sandstone, overlain by Namur Sandstone||
19796|Westbourne Formation|69681|6|Mentioned|p74 Fig.3, p82|Late Jurassic|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|69790|6|Mentioned|p1063 Fig.2, p1068 Fig.7|Late Jurassic|Late Jurassic|Eromanga Basin.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69797|5|Briefly described|p17 Fig.2|Late Jurassic|Late Jurassic|Geol. Prov: Eromanga Basin. Presented in figure as Westbourne Fm.||||||
19796|Westbourne Formation|69946|3|Fully described|p11, p15-16, p24, p57-58|Early Cretaceous|Late Jurassic|Named by Gerrard (1964) in an unpublished well completion report; Exon (1966) published the definition and assigned the type section: the interval 389.8 - 503.0m in Westbourne 1. Restricted to N Cooper region and easternmost Pedirka region in SA. 30 - 140m thick. Eromanga Basin. Wireline log correlations.||||Conformably overlies Adori Sandstone. Intertongues with overlying Namur and Algebuckina Sandstones.|Interbedded dark grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|69947|5|Briefly described|p7-8, p13 Fig.7.2, p31 Fig.7.20|Early Cretaceous|Late Jurassic|Eromanga Basin. Forms a couplet with Adori Sandstone, restricted to northern Cooper region and eastern-most Perdika region.||||Gradationally overlies Adori Sandstone. Is overlain by Namur Sandstone.|Dark grey shale, siltstone and minor sandstone interbeds.|
19796|Westbourne Formation|70374|6|Mentioned|p809 figure 1, p814|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Overlies ?conformably Springbok Sandstone.||28-SEP-16
19796|Westbourne Formation|70628|6|Mentioned|p952, Fig 4|Kimmeridgian|Kimmeridgian|Shown only as 'Westbourne' in fig 4. Along with Gubberamunda [Sandstone], Springbok Formation,  forms part of the L-sequence (Hoffman et al 2009) of the Surat Basin.||||Underlies Gubberamunda Sandstone. Overlies Springbok Formation.||
19796|Westbourne Formation|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Eromanga and Surat Basins. Aquitard.||Injune Creek Group.||Overlies Adori Sandstone and Springbok Sandstone. Is overlain by Namur Sandstone, Hooray Sandstone and Gubberamunda Sandstone.||
19796|Westbourne Formation|70823|5|Briefly described|p25-p27, p43, p78|Late Jurassic|Middle Jurassic|Eromanga Basin. Deposited in low-energy meandering fluvial and overbank floodplain environments.||||Overlies the Adori Sandstone. Overlain by the Namur Sandstone.||
19796|Westbourne Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Adori Sandstone. Overlain by the Murta Formation and the Hooray and Namur Sandstones.||
19796|Westbourne Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
19796|Westbourne Formation|71282|6|Mentioned|p457 Fig.1|||Appears just as Westbourne in Fig.1.||||||
19796|Westbourne Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
19796|Westbourne Formation|71342|4|Described|Ch1 p19, Ch5 p12, Ch5 p15-p17, Ch5 p24|Berriasian|Tithonian|Originally defined by Gerrard (1964) in the Boree 1 unpublished well completion report, however, it was first published by Exon (1966) who defined it and assigned the type section. The type section is in Westbourne 1 in Queensland (Exon, 1966). This unit is generally 30 to 140m thick in the Cooper region. Spore-pollen zone is given in Ch5 p57. Interpreted to have been deposited in a lacustrine environment. Sedimentary characteristics are briefly discussed. See also  Ch5 p57-p58, Ch7 p7-p8, Ch7 p13, Ch8 p5, Ch8 p10, Ch8 p17, Ch13 p4, Ch13 p9.||||Conformably overlies the Adori Sandstone. Conformably overlain by the Namur and Algebuckina Sandstones. This unit intertongues with, and is laterally equivalent to the Algebuckina Sandstone.|Interbedded darky grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
19796|Westbourne Formation|71863|6|Mentioned|p5|Valanginian|Berriasian|NE Eromanga Basin. Shown as "uppermost Westbourne Formation".||||||
19796|Westbourne Formation|72297|6|Mentioned|p739, p742|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential.||||||
19796|Westbourne Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Injune Creek Group.||Overlies Adori or Springbok Sandstone. Is overlain by Namur and Hooray Sandstones.||
19796|Westbourne Formation|72921|5|Briefly described|p15 Fig.2, p16.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland and the Eromanga Basin.||||Overlies and is laterally equivalent to Adori Sandstone and underlies Namur Sandstone and Hooray Sandstone.|May include siltstone.|
19796|Westbourne Formation|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 49, 66-67...|||Surat Basin. Tight aquitard. More locations: p. 69, 71, 78, 80, 98, 115-116, 119, 128-129, 148-149, 152, 167, 169-172, 177-178, 191.||||Underlain by Springbok Sandstone. Overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
19796|Westbourne Formation|73193|6|Mentioned|p369|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Underlain by Springbok Sandstone. Unconformably overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73200|6|Mentioned|p533|Jurassic|Jurassic|||||||
19796|Westbourne Formation|73251|6|Mentioned|p62|Late Jurassic|Late Jurassic|Eromanga Basin. Deposited in a braided-meandering fluvial setting. Oil show.||||Underlain by Adori Sandstone. Overlain by and equivalent to Namur Sandstone. Equivalent to Algebuckina Sandstone.||
19796|Westbourne Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Adori Sandstone. Overlain by Hooray Sandstone.||
19796|Westbourne Formation|73393|6|Mentioned|p20-21|Tithonian|Tithonian|Surat and Eromanga Basins.||Injune Creek Group||Underlain by Adori Sandstone. Underlain by and equivalent to Springbok Sandstone.||
19796|Westbourne Formation|73479|5|Briefly described|p156 Fig.2, p159|Jurassic|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 150 Ma|||Overlies Adori Sandstone, underlies Hooray Sandstone||
19842|Westmoreland Conglomerate|22538|6|Mentioned|P714||Statherian|||||||
19842|Westmoreland Conglomerate|22644|5|Briefly described|5|||Geol province McArthur Basin. Parent Murphy Metamorphics||||||
19842|Westmoreland Conglomerate|23065|6|Mentioned|4|||||||||
19842|Westmoreland Conglomerate|23066|5|Briefly described|p808|||Overlying unit Seigal Volcanics.||||||
19842|Westmoreland Conglomerate|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Tawallah Group.||||||07-NOV-08
19842|Westmoreland Conglomerate|23395|5|Briefly described|p395|||||||||
19842|Westmoreland Conglomerate|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
19842|Westmoreland Conglomerate|23867|5|Briefly described|Fig. 30|||Of Tawallah Group. Correlates with part of Mamadewerre Sandstone of the Kombolgie Subgroup (Katherine River Group).||||||
19842|Westmoreland Conglomerate|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Geological Province: McArthur Basin, Murphy Province.||||||07-NOV-08
19842|Westmoreland Conglomerate|26310|4|Described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Sandstone and conglomerate. Maximum Thickness: 4000 feet.||||||
19842|Westmoreland Conglomerate|29961|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|30318|6|Mentioned|p327|||||||||
19842|Westmoreland Conglomerate|30912|6|Mentioned|p364|||||||||
19842|Westmoreland Conglomerate|31348|4|Described|p345|||||||||
19842|Westmoreland Conglomerate|31421|6|Mentioned|p509|||||||||
19842|Westmoreland Conglomerate|31824|6|Mentioned|p28|||See also P32. U.Proterozoic||||||
19842|Westmoreland Conglomerate|32660|5|Briefly described|Table 4|||||||||
19842|Westmoreland Conglomerate|32758|6|Mentioned|p62|||||||||
19842|Westmoreland Conglomerate|33214|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|33225|6|Mentioned|p24|||||||||
19842|Westmoreland Conglomerate|34006|6|Mentioned|p64|||||||||
19842|Westmoreland Conglomerate|35114|6|Mentioned|p200|||||||||
19842|Westmoreland Conglomerate|35495|6|Mentioned|p340|||||||||
19842|Westmoreland Conglomerate|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|36012|3|Fully described|Table 2|||See also P11.||||||
19842|Westmoreland Conglomerate|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19842|Westmoreland Conglomerate|37568|5|Briefly described|p77|||||||||
19842|Westmoreland Conglomerate|38557|5|Briefly described|p293|||||||||
19842|Westmoreland Conglomerate|38584|4|Described|p11|||||||||
19842|Westmoreland Conglomerate|38902|6|Mentioned|p28|||||||||
19842|Westmoreland Conglomerate|39445|5|Briefly described|Table 2|||||||||
19842|Westmoreland Conglomerate|39497|6|Mentioned|p7|||See also Fig.4||||||
19842|Westmoreland Conglomerate|39685|6|Mentioned|Fig.1|||||||||
19842|Westmoreland Conglomerate|39986|6|Mentioned|p75|||||||||
19842|Westmoreland Conglomerate|40489|6|Mentioned|p89|||||||||
19842|Westmoreland Conglomerate|40491|6|Mentioned|p79|||||||||
19842|Westmoreland Conglomerate|40675|6|Mentioned|Table 1A|||||||||
19842|Westmoreland Conglomerate|40691|6|Mentioned|p9|||||||||
19842|Westmoreland Conglomerate|41125|6|Mentioned|p35|||See also Fig.21||||||
19842|Westmoreland Conglomerate|41319|4|Described|p195|||||||||
19842|Westmoreland Conglomerate|41594|6|Mentioned|p50|||||||||
19842|Westmoreland Conglomerate|41721|3|Fully described|p9|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Unconformably overlies Murphy Metamorphics (west), Nicholson Granite Complex (central area) and Cliffdale Volcanics (east). Conformably overlain by Seigal Volcanics. Thickness:1900m. Sandstone and conglomerate. Geol.prov: McArthur Basin||||||01-AUG-07
19842|Westmoreland Conglomerate|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
19842|Westmoreland Conglomerate|42385|6|Mentioned|p3|||||||||
19842|Westmoreland Conglomerate|42639|5|Briefly described|p8|||Stratigraphic equivalent to Yiyintyi Sandstone||||||
19842|Westmoreland Conglomerate|42812|5|Briefly described|p11|||see also Fig.5||||||
19842|Westmoreland Conglomerate|43010|5|Briefly described|Fig.6||Mesoproterozoic|of Tawallah Group. Of "Mid Proterozoic" age.||||||
19842|Westmoreland Conglomerate|43036|6|Mentioned|Fig.5|||||||||
19842|Westmoreland Conglomerate|43788|6|Mentioned|p14|||||||||
19842|Westmoreland Conglomerate|44271|2|Defined|p39,55,57||Paleoproterozoic|Overlies Cliffdale Volcanics and Nicholson Granite.||||||07-NOV-08
19842|Westmoreland Conglomerate|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
19842|Westmoreland Conglomerate|44275|14|Not recorded|Map Legend|||||||||
19842|Westmoreland Conglomerate|44280|2|Defined|p5-8,Tb.1,map|||||||||
19842|Westmoreland Conglomerate|44287|14|Not recorded|opp.p.7|||Equiv. of Yiyinti Sandstone. (E53-3).||||||
19842|Westmoreland Conglomerate|44305|14|Not recorded|p.6,8,11,19|||(E53-8). opp.6,18.||||||
19842|Westmoreland Conglomerate|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19842|Westmoreland Conglomerate|44473|14|Not recorded|p.7-8, opp. p.7|||(E53-7).||||||
19842|Westmoreland Conglomerate|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
19842|Westmoreland Conglomerate|44521|14|Not recorded|p1,7,9,10,13-15,46||Neoproterozoic|||||||
19842|Westmoreland Conglomerate|44751|14|Not recorded|p302|||The unit if older than the Neoproterozoic Constance Sandstone.||||||
19842|Westmoreland Conglomerate|44989|2|Defined|p.114-115|||Tb.II. On many pages. (E54,5) + NT. Pl.8,15.||||||
19842|Westmoreland Conglomerate|45162|3|Fully described|p11|Proterozoic|Proterozoic|||||||21-FEB-18
19842|Westmoreland Conglomerate|45166|5|Briefly described|p77|||||||||
19842|Westmoreland Conglomerate|45287|14|Not recorded|p.223,226,228,231|||||||||
19842|Westmoreland Conglomerate|46804|6|Mentioned|p154|||Stratigraphy||||||
19842|Westmoreland Conglomerate|49001|6|Mentioned|p4|||||||||
19842|Westmoreland Conglomerate|50536|6|Mentioned|p3.2|||Overlies: Nicholson Suite.||||||19-JUL-04
19842|Westmoreland Conglomerate|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
19842|Westmoreland Conglomerate|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Seigal Volcanics.||||||03-JUN-09
19842|Westmoreland Conglomerate|63109|6|Mentioned|p1111, p1108 Fig. 3, p1112|||Proximal fluvial sandstone. Geological Province: Leichhardt Superbasin.||||||30-SEP-08
19842|Westmoreland Conglomerate|63112|6|Mentioned|p1189-1191,p1193-1195,p1198,p1200-1206|||Leichhardt Superbasin. Framework grain dissolution after burial produced secondary porosity, allowing movement of basinal brines similar to those reported from Pb-Zn and U deposits of southern McArthur Basin. Age approximated from Fig.2. <2000 m thick.|c.1795-1790 Ma.||||Proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained.|
19842|Westmoreland Conglomerate|63113|6|Mentioned|p1225 Fig.13. |||Leichhardt Superbasin.||||||
19842|Westmoreland Conglomerate|63115|6|Mentioned|p1279 Fig.4.|||Base of Leichhardt superbasin. Potential aquifer sequence.||||||
19842|Westmoreland Conglomerate|63116|6|Mentioned|p1297 Fig.2, p1299-1306, p1309 |||Leichhardt superbasin. Material properties detailed. Aquifer.||||||
19842|Westmoreland Conglomerate|63866|5|Briefly described|p56|||||||(Possibly) equivalent to the Guide Supersequence.||
19842|Westmoreland Conglomerate|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p377  |||||Of the Tawallah Group.||||
19842|Westmoreland Conglomerate|65228|5|Briefly described|p7, Figs.02, 06, 07. |||Southern McArthur Basin.||Basal unit in Tawallah Group.||Is overlain by Seigal Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|65232|5|Briefly described|p9, p8 Fig. 7, p66-68, App. 2|Late Palaeoproterozoic|Late Palaeoproterozoic|At base of Tawallah Group. Conformably underlies Seigal Volcanics; unconformably over Cliffdale Volcanics. Thickness: up to 1800 m. Arenite, conglomerate, minor siltstone. Uranium mineralisation. Geol. Prov: McArthur Basin.||||||09-FEB-10
19842|Westmoreland Conglomerate|65337|6|Mentioned|pp12-13. |||Southern McArthur Basin. Correlative of Don Creek Sandstone.||||||
19842|Westmoreland Conglomerate|65340|5|Briefly described|p12 Fig.6, p84.|||McArthur Basin. Only occurs in the subsurface in this map area.||Unit at base of Tawallah Group.||Is overlain by Seigal Volcanics. Is shown as equivalent to Yiyintyi Sandstone.||23-MAR-18
19842|Westmoreland Conglomerate|66529|5|Briefly described|p20 Fig.7, p21  |||Basal unit in McArthur Basin. Over 1200 m thick. Hosts uranium deposits aged around 1655 Ma (Polito et al., 2005) along the Redtree dyke zone.||||Conformably overlain by the Seigal Volcanics.|Arkose, conglomerate and quartz arenites.|
19842|Westmoreland Conglomerate|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Is overlain by Seigal Volcanics.|Pebble and cobble conglomerate, lithic and quartz sandstone, red micaceous siltstone.|
19842|Westmoreland Conglomerate|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p9|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Leichhardt Superbasin. Informally subdivided into 5 units. Max depositional age: 1814 +/-14 Ma (Magee et al in prep).|1865 +/- 7 Ma and 1843 +/- 4 Ma MDAs.|Tawallah Group.||Correlated with Wire Creek Sandstone and Mount Guide Quartzite.|Pebble to cobble conglomerate, white argillaceous sandstone and orthoquartzite.|
19842|Westmoreland Conglomerate|67352|6|Mentioned|p15 Tb.2|||||||Is overlain conformably by Seigal Volcanics.||
19842|Westmoreland Conglomerate|67479|5|Briefly described|p2 Tb.1, pp12-15, p61 Tb.4, p62 Tb.4|Orosirian|Orosirian|Maximum depositional age.|1830 +/- 7 Ma.||||Silicified altered fine-grained pink tuff.|24-JAN-17
19842|Westmoreland Conglomerate|68020|5|Briefly described|p127|||Hosts uranium mineralisation near contact with overlying Seigal Volcanics.||||Unconformably overlain by Seigal Volcanics.|Sandstone and conglomerate.|
19842|Westmoreland Conglomerate|68575|4|Described|p2, p6-7, p87-93, p125, p134|||Mount Isa Region. A major component of the basement terrane in the Duchess and Dajarra 1:100 000 sheet areas. Thin section analysis showed the clasts are quartzo-feldspathic siliciclastics; zircons have detrital morphology; thus the rock is not a peperite. This means the age is of maximum deposition, not emplacement/deposition. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Kombolgie Subgroup; Depot Creek Sandstone). Whole rock Sm-Nd isotopic data and age (1819 Ma).|1815 +/- 14 Ma (maximum deposition age).|Kurbayia Metamorphic Complex.|||Fine-grained, subangular to angular clasts to 10cm in a siltstone matrix.|
19842|Westmoreland Conglomerate|68733|6|Mentioned|p186||Orosirian|Maximum depositional age of ca. 1830 Ma. Basal eastern McArthur Basin.||||||
19842|Westmoreland Conglomerate|69383|4|Described|p43-48, 49|Paleoproterozoic|Paleoproterozoic|Base of McArthur Basin. Fluvial. Up to 1400 m thick. Four upward-fining cycles. LA-ICPMS U-Pb and Hf geochronology analyses.  2 samples. Max deposition age is further constrained by underlying Murphy Metamorphics.|1865+/-7; 1843+/-4 Ma|||Unconformable on Murphy Metamorphics. Conformably overlain by Carolina Sandstone Member.|Coarse pebbly sandstone from the youngest, fourth cycle of the formation; Coarse pebbly conglomeritic sandstone for top of unit; sampled.|
19842|Westmoreland Conglomerate|69418|5|Briefly described|p3:19|||McArthur Basin. Hosts U deposits in sub-horizontal and sub-vertical lenses adjacent to altered, sub-vertical dolerite dykes.||||Unconformably overlies Cliffdale Volcanics.||12-JUL-16
19842|Westmoreland Conglomerate|69423|5|Briefly described|p8:1, 2 Fig.8.3, 5-6|||Separated by the Tin Hole Hinge Line, a probable thrust fault, from the Murphy Inlier to the S. Hosts a number of uranium +/- gold occurrences, and appears to be the source of numerous stream sediment gold occurrences.||||Unconformably overlies Cliffdale Volcanics.||12-JUL-16
19842|Westmoreland Conglomerate|69430|4|Described|p15:3, 9-11, 49-51|||Southern McArthur Basin. Up to 1900m thick. Fluvial to alluvial fan deposits, derived from the NE. Hosts small U-Au deposits (described in some detail).||Tawallah Group.||Unconformably overlies Cliffdale Volcanics, Nicholson Granite Complex and Murphy Metamorphics. Is overlain conformably by Seigal Volcanics. Probably equivalent to lower Kombolgie Subgroup.|A thick succession of conglomerate, coarse argillaceous sandstone with scattered pebbles.|12-JUL-16
19842|Westmoreland Conglomerate|69433|5|Briefly described|p18:2, 5|||McArthur Basin. Fluvial braided river and alluvial fan deposits.||Basal Tawallah Group.||Correlated with Wire Creek and Don Creek Sandstones (Lawn Hill Platform).||12-JUL-16
19842|Westmoreland Conglomerate|69434|6|Mentioned|p19:4|||Basal McArthur Basin. A possible source of siliciclastic sediments for the Caulfield beds, South Nicholson Basin.||||||12-JUL-16
19842|Westmoreland Conglomerate|69591|4|Described|p33-34, p39, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Fluvial deposits. Another maximum depositional age of 1843 +/- 4 Ma is by Carson et al. (2011).|1814 +/- 14 Ma (MDA: Magee et al. in press).|Basal Tawallah Group.||Is overlain by Seigal Volcanics. Correlated with Wire Creek Sandstone and Mount Guide Quartzite.|Pebble to cobble conglomerate, white argillaceous sandstone and orthoquartzite.|
19842|Westmoreland Conglomerate|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group||Overlain by Seigal Volcanics||
19842|Westmoreland Conglomerate|69917|4|Described|p199-201|Paleoproterozoic|Paleoproterozoic|McArthur Basin. U/Pb LA-ICPMS zircon dating. 1851+/-7.2 Ma is interpreted to be a conservative estimate of the maximum depositional age of this rock. This is slightly older than the age (1843+/-4 Ma) reported for the upper unit of the conglomerate (Hollis et al 2010a).Carson et al 2011 reported an age of 1830+/-7 Ma for a silicified tuff that forms a layer within the basal Westmoreland Conglomerate. This implies that sedimentation began after the maximum depositional age reported here.||||Unconformably overlies Cliffdale Volcanics. Correlated with Kombolgie Subgroup.|coarse-grained sandstone composed of quartz grains in a kaolinite matrix. Bed bases are marked by cobble beds between 0.05 and 0.2 m thick.|
19842|Westmoreland Conglomerate|70284|5|Briefly described|p1243, p1245-1252, p1255-1258|Statherian|Statherian|McArthur Basin, Leichhardt Superbasin. Up to 1800m thick. Hosts uranium mineralization.|> 1680+/-18 Ma (fluid migration age)|||Conformably overlain by Seigal Volcanics. Cut by dolerite dykes.|Quartz, chert and felsic volcanic cobble conglomerate and medium-coarse grained, well sorted sandstone.|14-DEC-16
19842|Westmoreland Conglomerate|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin. Five facies are mapped separately.||Tawallah Group.||Unconformably overlies Cliffdale Volcanics. Is overlain by Seigal Volcanics.|Siltstone, conglomerate and talus breccia, sandstone; pebble and cobble conglomerate, sandstone; boulder and cobble conglomerate, greywacke, sandstone; conglomerate, sandstone, greywacke, siltstone.|
19842|Westmoreland Conglomerate|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1830+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Coarse-grained sandstone, rhyodacite, coarse pebbly sandstone, volcanic rock.|
19842|Westmoreland Conglomerate|71799|5|Briefly described|p150 fig 2|Statherian|Orosirian|McArthur Basin.|ca. 1800 Ma|||Overlain by the Seigal Volcanics.|Sandstone, greywacke and conglomerate.|
19842|Westmoreland Conglomerate|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Orosirian|Shown as located in the Southeastern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age. Shown on diagram as Statherian age but depositional ages listed are Orosirian.|1830 +/-7 Ma, to 1815 +/-7 Ma|Tawallah Group||Shown as unconformably overlying Nicholson Granite Complex and Cliffdale Volcanics and partially underlies Seigal Volcanics.||
19842|Westmoreland Conglomerate|72527|5|Briefly described|p161, p177, p194.|Paleoproterozoic|Paleoproterozoic|The siliclastic detritus generated by this unit is thought to contribute to the Caulfield beds.||||Equivalent to Wire Creek Sandstone.||
19842|Westmoreland Conglomerate|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||Tawallah Group||Overlain by Seigal Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11.|Statherian|Statherian|Located in the Southeastern McArthur Basin, in the Southern McArthur Basin. Two U-Pb zircon sedimentary depositional ages given 1830+/-7 Ma, 1815+/-7 Ma.||Tawallah Group||Unconformably overlies Nicholson Granite Complex and Cliffdale Volcanics. Equivalent to Yiyintyi Sandstone.||
19842|Westmoreland Conglomerate|72919|6|Mentioned|p12|||Intersected in drillhole BEN-SD60.||Tawallah Group||||
19842|Westmoreland Conglomerate|73042|6|Mentioned|p4||Orosirian|Southern McArthur Basin, Leichhardt Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1830 +/- 7 Ma, 1815 +/- 7 Ma (see Fig.1.2)|Tawallah Group||Partly unconformably underlain(?) by Nicholson Granite Complex. Overlain by Seigal Volcanics.||
19842|Westmoreland Conglomerate|73412|5|Briefly described|p2, 4, 8, 12|||The basal unit in the southern McArthur Basin. Smooth, non-magnetic response.||Tawallah Group.||Lateral equivalent to Yiyintyi Sandstone. Is overlain by Seigal Volcanics.||
19849|Westwood Complex|30811|6|Mentioned|p528|||West mass of Bouldercombe Complex||||||
19849|Westwood Complex|41924|6|Mentioned|p28|||||||||
19849|Westwood Complex|68008|5|Briefly described|p341, p436|||Wood (1974), Ford et al. (1976); for the western lobe of the Bouldercombe Complex. Wood (1974) subdivided it into three major intrusive phases: southern and northern tonalites and granodiorite transitional to granite; these are defined in this study as the Flaggy Quartz Monzodiorite, Umbrella Granodiorite and Moonkan Granite respectively.||||||
19853|Wetheron Basalt|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Of the Aranbanga Volcanic Group.||||||05-MAR-08
19853|Wetheron Basalt|41738|2|Defined|p170|Late Triassic||Reserved as Wetheron.||||||18-AUG-08
19853|Wetheron Basalt|41790|5|Briefly described|p474|||||||||
19853|Wetheron Basalt|42054|6|Mentioned|p272|||||||||
19853|Wetheron Basalt|63821|5|Briefly described|p21|Late Triassic|Late Triassic|Part of the Aranbanga Volcanic Group. Age" 221.2+/-5.8Ma. (K-Ar radioemtric). Amygdaloidal olivine basalt locally containing abundant, very large plagioclase phenocrysts.||||||07-FEB-11
19853|Wetheron Basalt|68679|4|Described|p437, p439-440|Late Triassic|Late Triassic|Cranfield (1989). Gayndah region, northern New England Orogen. Up to ~30m thick in lava-filled valleys.|221.2 +/- 5.8 Ma (K-Ar plag.: Stephens, 1991).|Aranbanga Volcanic Group.||Overlies Woodmillar Andesite and Beeswing Rhyolite.|Fine-grained, coarsely porphyritic amygdaloidal basalt; basalt to dacite, calcite- and siderite-filled amygdales up to 10mm diameter.|
19853|Wetheron Basalt|73450|5|Briefly described|p30, p34-35|Norian|Norian|K-Ar age of 221.2 +/- 5.8 Ma (Stephens, 1991).|221.2 +/- 5.8 Ma K-Ar|Aranbanga Volcanic Group|||Coarsely porphyritic amygdaloidal basaltic lavas.|
19856|Weymouth Granite|22811|6|Mentioned|p604|Permian|Permian|U/Pb zircon date 284 Ma||||||
19856|Weymouth Granite|23420|5|Briefly described|p 147 table 4.6|Permian|Late Carboniferous|Also see p130. In the Weymouth Supersuite of the Cape York Penninsula Batholith. Age: 285Ma.||||||
19856|Weymouth Granite|23425|5|Briefly described|p372|||||||||
19856|Weymouth Granite|23430|5|Briefly described|p510|||||||||
19856|Weymouth Granite|23431|5|Briefly described|p535|||||||||
19856|Weymouth Granite|30257|6|Mentioned|p286|||See also P290 for date||||||
19856|Weymouth Granite|30914|6|Mentioned|Map legend|Permian|Permian|||||||
19856|Weymouth Granite|32528|5|Briefly described|Table 2|||||||||
19856|Weymouth Granite|32563|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19856|Weymouth Granite|33226|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19856|Weymouth Granite|33770|6|Mentioned|p520|||||||||
19856|Weymouth Granite|33773|4|Described|Table 1|||||||||
19856|Weymouth Granite|33880|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19856|Weymouth Granite|33882|4|Described|Table 1|||P13||||||
19856|Weymouth Granite|34581|2|Defined|p138|Permian|Permian|See also PP130,132,140||||||
19856|Weymouth Granite|34582|6|Mentioned|p535|||Lower Permian.||||||
19856|Weymouth Granite|39445|5|Briefly described|Table 12|||||||||
19856|Weymouth Granite|42327|6|Mentioned|Fig. 22 P15|||||||||
19856|Weymouth Granite|42550|4|Described|p8|||||||||
19856|Weymouth Granite|42640|5|Briefly described|p10|||||||||
19856|Weymouth Granite|42650|6|Mentioned|p15|||||||||
19856|Weymouth Granite|42769|6|Mentioned|p11|||||||||
19856|Weymouth Granite|43124|5|Briefly described|p31|||||||||
19856|Weymouth Granite|43567|5|Briefly described|p402,403|Permian|Carboniferous|||||||
19856|Weymouth Granite|43725|5|Briefly described|p1-3|||U-Pb age: 287+/-8 Ma||||||
19856|Weymouth Granite|43741|5|Briefly described|p11|Permian|Carboniferous|||||||
19856|Weymouth Granite|43811|6|Mentioned|Fig.1,p192,193|||||||||
19856|Weymouth Granite|45076|3|Fully described|p121|||L.Perm.  See also P17.||||||
19856|Weymouth Granite|49769|6|Mentioned|Fig.1,p2|||||||||
19856|Weymouth Granite|69591|5|Briefly described|p101-102|Permian|Permian|Dykes of this unit intrude and metamorphose rocks of the Pascoe River Basin. Is overlain by rocks of the (subsurface) Olive River Basin.||||Intrudes Pascoe River beds.||
19856|Weymouth Granite|69592|5|Briefly described|p282|||Age of an unnamed granite formerly part of this unit.|409 +/- 6 Ma (SHRIMP U-Pb zircon).|||||
19856|Weymouth Granite|69593|5|Briefly described|p475, p477 Tb.6.2, p512|||There is a zone of hybrid rocks along the western margin of this unit. Sm-Nd isotope data tabulated.|287-284 Ma.|Weymouth Supersuite.|||I-type.|
19856|Weymouth Granite|70207|5|Briefly described|p125-126|Permian|Permian||~285 Ma.|||Intrudes Sefton Metamorphics.||
19856|Weymouth Granite|71592|5|Briefly described|Appendix A.|||Kennedy igneous Province.|284+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
19856|Weymouth Granite|71792|6|Mentioned|p15, p27-p28, p33, p37, p44, p48, p51|Early Permian|Early Permian|Also referred to as the Cape Weymouth Granite on p27.||||Intrudes the Janet Ranges Volcanics. Appears to be intruded by the Kennedy Hill Granite.|Porphyritic biotite granite, some microgranite.|
19856|Weymouth Granite|71849|4|Described|p2, p5, p11, p51, p111, p114, p143-144|Permian|Permian|Previously mapped Early Permian I-type granitoids in northern Coen Inlier. Possible epithermal gold mineralisation in associated volcanic rocks. U-Pb zircon SHRIMP ages.|287 +/- 8 Ma and 284 +/- 4 Ma.||Ebagoola, Lankelly Suites.||S-type.|
19856|Weymouth Granite|71853|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||Porphyritic biotite granite, some microgranite.|
19856|Weymouth Granite|71854|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||Porphyritic biotite granite, some microgranite.|
19856|Weymouth Granite|72983|6|Mentioned|p4, p60, p66-67|Kungurian|Asselian|Ages from Black et al. (1992). Strong temporal relationship with the Janet Ranges Volcanic Group. Age is within uncertainty of that of Wolverton Granite and Twin Humps Granite.|287 +/- 8 Ma, 284 +/- 4 Ma SHRIMP U-Pb|Weymouth Supersuite||Intrudes Janet Ranges Volcanic Group.||
19856|Weymouth Granite|73083|6|Mentioned|p56-57|Permian|Permian|||||||
19861|Wharleys Tonalite|22847|3|Fully described|p 49|Early Devonian|Silurian|||||||
19861|Wharleys Tonalite|23422|5|Briefly described|p191, p213 Table 6.8|||||||||
19861|Wharleys Tonalite|42633|5|Briefly described|Table 1 P8|||Reserved as Wharleys Granodiorite.||||||
19861|Wharleys Tonalite|42750|2|Defined|p42|Early Devonian|Late Silurian|||||||
19861|Wharleys Tonalite|43093|4|Described|Appendix 1|Early Devonian|Silurian|Middle Silurian to Early Devonian age.||||||
19861|Wharleys Tonalite|43934|5|Briefly described|Map Legend|Devonian|Silurian|||||||
19861|Wharleys Tonalite|62075|6|Mentioned|p15 Fig.7|||Ravenswood batholith. Appears as Wharleys ton.||Unit in Millchester Supersuite.||||
19861|Wharleys Tonalite|62521|5|Briefly described|p55|||Of Millchester Creek Supersuite. Geological Province: Ravenswood Batholith. See also Wharleys Granodiorite.||||||14-JAN-08
19883|Whitdale Granodiorite|42747|5|Briefly described|Fig.9, Table 1|||same as Whitdale Granite||||||
19883|Whitdale Granodiorite|43029|2|Defined|p23||Devonian|see also Fig.2,p16||||||
19883|Whitdale Granodiorite|43204|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|||||||23-DEC-11
19883|Whitdale Granodiorite|43213|3|Fully described|p96-98, p104-105, p111, p116-121, p141|Late Devonian|Late Devonian|See also p175, p179, p209-210, p226, p234, p241. Type locality described. Component of the Retreat Batholith. This relatively young age may be due to resetting by the emplacement of Mount Newsome Granodiorite. Peraluminous. Geochemistry, modal and chemical analyses, geophysics and deformation structures detailed. Appears as Whitdale Granite on p209.|370 Ma (K-Ar biotite: Webb and McDougall, 1968).|||Intrudes Anakie Metamorphic Group and Gem Park Granite. Is intruded by Mount Newsome Granodiorite. Is overlain unconformably by Silver Hills Volcanics.|Grey, foliated and lineated medium- to coarse-grained, porphyritic biotite granodiorite, characterised by large, aligned pink alkali feldspar phenocrysts.|
19883|Whitdale Granodiorite|68731|6|Mentioned|p135|||Minimum age constrained by the intrusive Mount Newsome Granodiorite.|> 392.4 +/- 10.2 Ma, U-Pb (SMRIMP)|||Intruded by the Mount Newsome Granodiorite.||13-MAY-16
19883|Whitdale Granodiorite|70856|5|Briefly described|Map Legend|Late Devonian|Middle Devonian||||||Grey, foliated and lineated, medium- to coarse-grained, porphyritic biotite granodiorite.|
19912|White Springs Complex|22533|6|Mentioned|p54|Early Devonian|Silurian|placed in Pama Province||||||
19912|White Springs Complex|33909|6|Mentioned|p230|||Refers Bain et al 1975||||||
19932|Whitsunday Volcanics|23427|5|Briefly described|Table 11.2 p418.|||||||||
19932|Whitsunday Volcanics|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19932|Whitsunday Volcanics|31659|5|Briefly described|p76|Cretaceous|Cretaceous|Intermediate and acid pyroclastics and flows.||||||08-OCT-08
19932|Whitsunday Volcanics|32357|6|Mentioned|p7|||||||||
19932|Whitsunday Volcanics|32553|4|Described|p38|||||||||
19932|Whitsunday Volcanics|32554|4|Described|Table 2|||||||||
19932|Whitsunday Volcanics|32555|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19932|Whitsunday Volcanics|34408|6|Mentioned|p185|||On table||||||
19932|Whitsunday Volcanics|35460|6|Mentioned|p152|||||||||
19932|Whitsunday Volcanics|36472|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19932|Whitsunday Volcanics|36906|5|Briefly described|Fig.2|||||||||
19932|Whitsunday Volcanics|36961|6|Mentioned|Table 1|||||||||
19932|Whitsunday Volcanics|37675|6|Mentioned|Fig.2|||||||||
19932|Whitsunday Volcanics|39445|5|Briefly described|Table 11|||||||||
19932|Whitsunday Volcanics|40245|6|Mentioned|p189|||||||||
19932|Whitsunday Volcanics|40574|6|Mentioned|p5|||||||||
19932|Whitsunday Volcanics|41246|6|Mentioned|Map legend|Cretaceous||||||||
19932|Whitsunday Volcanics|42660|6|Mentioned|App.3.1 p165|||||||||
19932|Whitsunday Volcanics|45151|5|Briefly described|p17|||See also Table 12.||||||
19932|Whitsunday Volcanics|48921|2|Defined|p33|Early Cretaceous|Early Cretaceous|Table 2 on P33.||||||
19932|Whitsunday Volcanics|60473|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Mainly extensively weathered, mottled red and white, felsic tuff and/or volcaniclastic sandstone and siltstone.||||||
19932|Whitsunday Volcanics|61035|6|Mentioned|p18|Early Cretaceous|Early Cretaceous|Volcanic rocks. Geological Province: Coastal Block.||||||07-FEB-11
19932|Whitsunday Volcanics|61916|5|Briefly described|Map legend|Cretaceous|Cretaceous|Rhyolitic to andesitic volcaniclastic rocks, including ignimbrite, minor flows, conglomerate and sandstone. Overlie the Campwyn Volcanics.||||||
19932|Whitsunday Volcanics|63892|6|Mentioned|p208|||Text refers to 'Minor intrusive igneous rocks in the ODP holes may be Whitsunday Volcanics eqivalents but other correlations are also possible.||||||28-MAY-08
19932|Whitsunday Volcanics|64570|5|Briefly described|p855, p858|Early Cretaceous|Early cretaceous|Age: 114 (112)Ma. Mainly pyroclastics.||||||22-DEC-08
19932|Whitsunday Volcanics|65388|3|Fully described|p218-220, p219, p59, p403, p412|Early Cretaceous|Early Cretaceous|Defined: Clarke & others (1971) from the Whitsunday and Cumberland Groups of islands offshore from Proserpine. Studied  by Ewart & others (1992) and Bryan & others (1997, 2000). Dominated volumetrically by welded dacitic-rhyolitic lithic-rich ignimbrite. K-Ar dating of hornblende: 115+/-3 Ma (1971), SHRIMP dating elsewhere: 137.5+/-1.4 Ma. Unclear if volcanic activity spanned whole time or  K-Ar dates may be partially reset. Intruded by Mount Bassett Dolerite?||||||
19932|Whitsunday Volcanics|65706|4|Described|p12, p16 Tb.1, p18 Tb.1, p46, p49 |Early Cretaceous|Early Cretaceous|Hosts subeconomic Au-Ag mineralisation at Brandy Creek, and some minor Cu mineralisation. Extensively faulted. Comagmatic volcanic plug on Pentecost Island.||||Faulted against Airlie Volcanics.|Rhyolitic to andesitic volcaniclastic rocks, ignimbrite and flow, conglomerate, sandstone, hydrothermally altered quartz-feldspar porphyry.|
19932|Whitsunday Volcanics|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Whitsunday Province. This unit, as well as the Proserpine Volcanics and unnamed volcanic units, are all mapped under the symbol, Kv.||||||
19932|Whitsunday Volcanics|68679|6|Mentioned|p431|||Whitsunday-Proserpine area.||||||
19932|Whitsunday Volcanics|69594|5|Briefly described|p553-554, p558, p567|Early Cretaceous|Early Cretaceous|Clarke et al. (1971). Whitsunday Volcanic Province. >1km thick sequence. Forms most of the offshore islands along a strike distance of >300km. Coeval with Proserpine Volcanics. Lithologies and vulcanism very detailed. Middle Triassic and Early Cretaceous granites are exposed.|137.5 +/- 1.4 Ma (SHRIMP: Fanning et al. 2009).|||Contiguous with Proserpine Volcanics.|Silicic to intermediate pyroclastic rocks and minor lavas; silicic dykes; ignimbrite sheets with coarse, lithic-lag breccias; associated with caldera eruptive centres.|
19932|Whitsunday Volcanics|69742|6|Mentioned|p787, 792|Cretaceous|Cretaceous|A silica dominated large igneous province. Likely source of silica for opal in Winton Formation, Finch Claystone, Bulldog Shale. Shown as Whitsunday volcanics p787.|132-95 Ma|||||
19932|Whitsunday Volcanics|69952|6|Mentioned|p79-80|Early Cretaceous|Early Cretaceous|Murray (1975) had suggested this unit correlated with Double Mountain Volcanics. These latest age determinations show the latter's age (c.271 Ma) rules out that equivalence.||||||
19932|Whitsunday Volcanics|71592|5|Briefly described|Appendix A.||||138+/-1.4 Ma (SHRIMP U-Pb zircon).||||Ignimbrite.|
19932|Whitsunday Volcanics|71702|6|Mentioned|p177 Table 1|Cretaceous|Cretaceous||125.4+/-1.6 Ma eruption age from 1 sample.|||||
19932|Whitsunday Volcanics|73422|5|Briefly described|p2, p5-8, p12|||[Misspelt as Whitsuday Volcanics, p2]. Whitsunday Igneous Province, northern. Exposed in the Whitsunday Islands. At least 2 km thick. Province developed between 132 and 95 Ma based on K-Ar and Rb-Sr dating by Bryan and Purdy (2013).|||||Includes felsic to mafic lava flows, and obsidian tuffs.|
19932|Whitsunday Volcanics|73450|5|Briefly described|p3, p5|Cretaceous|Cretaceous|Calc-alkaline compositions; inherited from crustal sources as a result of large-scale crustal melting. Do not contain any rocks with (near-)peralkaline compositions. Associated with continental rifting and Whitsunday Silicic Large Igneous Province (Bryan et al., 1997, 2012).|||||Welded dacitic and rhyolitic ignimbrites intercalated with basaltic and silicic lavas.|
19932|Whitsunday Volcanics|73570|6|Mentioned|p914, p915 Fig.4, p916, p918-919|Early Cretaceous|Early Cretaceous|Yarrol Belt.|||||Includes siliciclastic units.|
19936|Whitula Formation|23982|6|Mentioned|p97 Appendix 13|||Geological Province: Great Artesian Basin.||||||
19936|Whitula Formation|33078|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|33079|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19936|Whitula Formation|35793|6|Mentioned|Fig.2|||||||||
19936|Whitula Formation|37607|6|Mentioned|Fig.4|||||||||
19936|Whitula Formation|38226|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|39445|5|Briefly described|Table 14|||||||||
19936|Whitula Formation|39478|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|40739|6|Mentioned|p589|||||||||
19936|Whitula Formation|41198|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|42375|5|Briefly described|Table 1 P11|||In Waite Basin. Previously used in Qld.||||||19-DEC-06
19936|Whitula Formation|42543|6|Mentioned|p6|||SA.||||||
19936|Whitula Formation|42746|6|Mentioned|p18|||||||||
19936|Whitula Formation|44041|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|44133|5|Briefly described|p190 Fig. 10.30|Early Pliocene|Late Miocene|||||||
19936|Whitula Formation|46802|6|Mentioned|Table 1|||||||||
19936|Whitula Formation|46854|6|Mentioned|Fig.1|||||||||
19936|Whitula Formation|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
19936|Whitula Formation|60080|5|Briefly described|Map legend|Pliocene|Miocene|Sandstone, siltstone, mudstone, and claystone, oxidised; minor gypsum and immature silcrete.  Overlies Glendower Formation; underlies Cadelga Limestone.||||||20-AUG-04
19936|Whitula Formation|61155|5|Briefly described|p17|Late Pliocene|Middle Miocene|Deposited in synclinal basins in southwest Queensland. Overlies the Cadelga Limestone. Age: 12-2Ma. Thickness: 220m. See also p4, p5.||||||
19936|Whitula Formation|64047|2|Defined|p61|Late Miocene|Late Miocene|Unconformably overlies Glendower Fm. or weathered Winton Fm. Overlain by Quaternary alluvium. Max. thickness: 160m. Contains interbedded quartzose sandstone, siltstone, mudstone and claystone with minor conglomerate; lignite and gypsum also present.||||||16-APR-08
19936|Whitula Formation|66131|6|Mentioned|p242 Fig.2, p245, p254|Miocene|Miocene|Senior and Mabbutt (1979) place the Cadelga Limestone and the Doonbara Formation at the top of this unit. Middle to Late Miocene in age (from Fig.2 - stratigraphic correlation chart).|||Includes Cadelga Limestone and Doonburra Formation.|||
19936|Whitula Formation|69599|5|Briefly described|p584, p599-602, p651|Miocene|Miocene|Senior et al. (1978). Eromanga, Lake Eyre Basins. Mostly known from drill holes. 53-160m thick. Fluviatile to lacustrine deposits. No fossils known. RELATED UNITS (continued): Also correlated (at least partly) with Horse Creek, Noranside, Austral Downs Limestones.||||Unconformably overlies Glendower and Winton Formations. Is overlain by Cadelga Limestone. Correlated with Doonbara, Poodyea Formations; and Mount Coley Sinter; see COMMENTS for more.|Interbedded quartzose sandstone, siltstone, mudstone and conglomerate; gypsiferous and lignitic in part.|
19936|Whitula Formation|70821|5|Briefly described|p25, p82|Miocene|Oligocene|Senior and Johnston (1974). Lake Eyre Basin (SA). Hydrostratigraphic properties.||||Equivalent to Namba Formation.||
19936|Whitula Formation|70823|5|Briefly described|p47|Pliocene|Late Oligocene|Maximum thickness of 160m.|ca 28 Ma||||Clay, fine-grained sand, carbonate and minor conglomerate.|17-SEP-18
19939|Whitworth Quartzite|22438|6|Mentioned|p549, Fig.12|||||||||
19939|Whitworth Quartzite|22585|5|Briefly described|Fig2 P737, Fig3|||Actually written as Whitworth Qtz.||||||19-DEC-06
19939|Whitworth Quartzite|23395|5|Briefly described|p386 Fig.3|||Of the Myally Subgroup.||||||19-DEC-06
19939|Whitworth Quartzite|23396|5|Briefly described|p407 Fig.2|||Of the Myally Subgroup (Haslingden Group).||||||19-DEC-06
19939|Whitworth Quartzite|30529|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslingden Group).  Overlies the Bortala Formation.||||||25-AUG-04
19939|Whitworth Quartzite|30534|2|Defined|p304|Precambrian|Precambrian|||||||
19939|Whitworth Quartzite|33900|4|Described|p12|||||||||
19939|Whitworth Quartzite|36226|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|38232|6|Mentioned|p84|||See also p89.||||||19-DEC-06
19939|Whitworth Quartzite|38448|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|39445|5|Briefly described|Table 2|||See also p40.||||||19-DEC-06
19939|Whitworth Quartzite|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Myally Subgroup (Haslinden Group). Feldspathic quartzite, purple sandstone, mudflake conglomerate; feldspathic quartzite, orhtoquartzite, labile sandstone; sandstones, siltstones, mudstones||||||15-JUN-06
19939|Whitworth Quartzite|39622|6|Mentioned|Fig.2|||||||||
19939|Whitworth Quartzite|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
19939|Whitworth Quartzite|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
19939|Whitworth Quartzite|40221|3|Fully described|p10|||||||||
19939|Whitworth Quartzite|40623|5|Briefly described|p99|||||||||
19939|Whitworth Quartzite|41298|6|Mentioned|Map legend|Carpentarian||||||||
19939|Whitworth Quartzite|41307|4|Described|p10|||||||||
19939|Whitworth Quartzite|42166|6|Mentioned|p110|||||||||
19939|Whitworth Quartzite|42523|5|Briefly described|Fig. 2 P373|||||||||
19939|Whitworth Quartzite|45136|5|Briefly described|p49|||||||||
19939|Whitworth Quartzite|45166|5|Briefly described|p14|||||||||
19939|Whitworth Quartzite|46801|6|Mentioned|Fig. 14|||||||||
19939|Whitworth Quartzite|47083|4|Described|p7-8|||Contains three informal members. Of Myally Subgp (Haslingden Gp). Conformably overlain by Lochness Fm. Conformably underlain by Bortala Fm.||||||19-DEC-06
19939|Whitworth Quartzite|50332|6|Mentioned|p17|Proterozoic|Proterozoic|Of the Myally Subgroup.||||||07-FEB-11
19939|Whitworth Quartzite|50536|6|Mentioned|p7.2|||Geological Province: Mount Isa Inlier.||||||
19939|Whitworth Quartzite|61929|5|Briefly described|p128 Fig. 2|||Of the Myally Subgroup.||||||
19939|Whitworth Quartzite|61936|6|Mentioned|p203|||Hosts the Mammoth Cu deposit. Geological Province: Leichhardt Superbasin (Mount Isa Inlier).||||||19-DEC-06
19939|Whitworth Quartzite|62988|5|Briefly described|p34|||Geological Province: Mount Isa Inlier.||||||25-JAN-07
19939|Whitworth Quartzite|63023|5|Briefly described|p1025 Fig. 2, p1029|Paleoproterozoic|Paleoproterozoic|Of Myally Subgroup (Haslingden Group). Age: 1768+/-8Ma. Overlies Bortala Formation; underlies Lochness Formation. Geological Province: Leichardt Superbasin. Pink, fine-grained, well-sorted sandstone. See also p1027 Tb. 1.||||||07-NOV-08
19939|Whitworth Quartzite|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Lochness Formation, underlain by Bortala Formation. Geological Province: Leichhardt Superbasin. Consists of sandstone.||||||
19939|Whitworth Quartzite|63111|5|Briefly described|p1163 Fig. 3, p1164 Tb. 1|Statherian|Statherian|Of Myally Subgroup. Overlain by Lochness Formation, underlain by Bortalla Formation. Age: 1768+/-8Ma. Geological Province: Leichhardt Superbasin. Consists mostly of sandstone.||||||07-FEB-11
19939|Whitworth Quartzite|63113|5|Briefly described|p1214 Fig.2, p1225 Fig.13.|||||Of the Myally Subgroup||Overlies Bortala Formation. Is overlain by Lochness Formation.||
19939|Whitworth Quartzite|63114|5|Briefly described|p1253 Fig.2. |||||Of the Myally Subgroup||Overlies Bortala Formation. Is overlain by Lochness Formation.||
19939|Whitworth Quartzite|63115|6|Mentioned|p1279 Fig.4.|||Leichhardt superbasin.||||||
19939|Whitworth Quartzite|63116|6|Mentioned|p1297 Fig.2, |||Leichhardt superbasin. Material properties detailed.||||||
19939|Whitworth Quartzite|63866|5|Briefly described|p58|||Leichhardt Superbasin.||Myally Supersequence||||
19939|Whitworth Quartzite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Mount Isa Inlier, Leichhardt Superbasin.|1768 +/- 8 Ma (maximum depositional age).|Myally Subgroup.|||Massive medium to coarse feldspathic to quatzose sandstone, fine purple sandstone and mudflake conglomerate|
19939|Whitworth Quartzite|68020|5|Briefly described|p126||||c. 1760 Ma|Myally Subgroup|||Brittle feldspathic quartzite.|
19939|Whitworth Quartzite|68732|5|Briefly described|p160, p161, p165 Fig.3|Statherian|Statherian|Shoreline facies deposited above fair-weather wave base. Of the Myally Supersequence. Maximum sedimentary depositional age.|1768 +/- 8 Ma|Of the Haslingden Group.|||Fine- to coarse-grained quartzites and arenites, fining upwards into thinly bedded sandstones.|01-DEC-17
19939|Whitworth Quartzite|69222|5|Briefly described|p222 Fig.2|Statherian|Statherian|Leichhardt River Fault Trough.||Myally Subgroup||Overlies Pickwick Metabasalt||09-FEB-18
19939|Whitworth Quartzite|69591|5|Briefly described|p33, p57|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin. Part of Myally Supersequence. Tide-dominated shelf/aeolian deposits.|1768 +/- 8 Ma (MDA: Neumann et al., 2006).|Myally Subgroup.|||Massive medium to coarse feldspathic to quartzose sandstone, fine purple sandstone and mudflake conglomerate.|
19939|Whitworth Quartzite|70348|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Bortala Formation. Is overlain by Lochness Formation.|Massive medium- to coarse-grained feldspathic to quartzose sandstone, fine-grained purple sandstone and mudflake conglomerate. (Separately mapped) white to pink feldspathic sandstone; minor siltstone.|
19939|Whitworth Quartzite|70352|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||Myally Subgroup.||Overlies Bortala Formation. Is overlain by Lochness Formation.|Massive medium- to coarse-grained feldspathic to quartzose sandstone, fine-grained purple sandstone and mudflake conglomerate. (Separately mapped) white to pink feldspathic sandstone; minor siltstone.|
19939|Whitworth Quartzite|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1768+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
19939|Whitworth Quartzite|71980|5|Briefly described|map legend sheet 1|Proterozoic|Proterozoic|From base: Coastal onlap including washover facies; subtidal shelf; coastal offlap, coarsening up shoreface.||Of Myally Subgroup|||Arkose, felspathic sandstone, quartz arenite;|
19939|Whitworth Quartzite|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Lochness Formation and is shown to partially underlie Quilalar Formation.||
19939|Whitworth Quartzite|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Lawn Hill Platform and Leichhardt River Fault Trough of the Mount Isa Province.||Myally Subgroup||Overlies Lochness Formation and is shown to partially underlie Quilalar Formation.||
19939|Whitworth Quartzite|72919|6|Mentioned|p63|||||Myally Subgroup, Myally Supersequence||||
19939|Whitworth Quartzite|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Mount Isa Province, Leichhardt Superbasin.||Myally Subgroup||Underlain by Lochness Formation. Partly overlain(?) Quilalar Formation.||
19939|Whitworth Quartzite|73525|6|Mentioned|p4-5 Fig.2, p19 Fig.13|||Leichhardt River Domain.|||||Clastics.|
19954|Whypalla Supersuite|12575|6|Mentioned|p781. |Permian|Permian|Early Permian S-type granites along the eastern side of Hodgkinson Province.|||Includes Mareeba, Mount Carbine, Cannibal Creek and Mount Pike Granites.|||
19954|Whypalla Supersuite|22497|6|Mentioned|p113|||||||||
19954|Whypalla Supersuite|23422|5|Briefly described|Plate 7.3|Early Permian|Early Permian|||||||
19954|Whypalla Supersuite|23423|4|Described|p312 Table 7.4||Early Permian|I-type granites. Age: 282 +/- 9 Ma (Rb-Sr). Also see p247.||||||
19954|Whypalla Supersuite|23430|5|Briefly described|p490|||Kennedy Province||||||
19954|Whypalla Supersuite|23431|5|Briefly described|p539|||S-type granite||||||
19954|Whypalla Supersuite|23497|6|Mentioned|p34|||||||||
19954|Whypalla Supersuite|23506|5|Briefly described|Map Legend||Early Permian|||||||
19954|Whypalla Supersuite|23616|5|Briefly described|p77||Permian|Isotopic age 275 Ma-285 Ma.  Hodgkinson Province.||||||02-JUN-09
19954|Whypalla Supersuite|24086|5|Briefly described|p312 Fig. 1|Early Permian|Early Permian|||||||
19954|Whypalla Supersuite|24213|5|Briefly described|p777|Permian|Permian|Intrudes the Hodgkinson Formation||||||
19954|Whypalla Supersuite|42658|4|Described|p31|||Variation on Whypalla Granite?||||||
19954|Whypalla Supersuite|42968|5|Briefly described|p99|||||||||
19954|Whypalla Supersuite|43060|4|Described|p105|||||||||
19954|Whypalla Supersuite|43083|4|Described|p127|||Includes Cannibal Creek and Nangee Granites. S-type. Mildly peraluminous.||||||17-JUN-09
19954|Whypalla Supersuite|43098|6|Mentioned|p31|||||||||
19954|Whypalla Supersuite|43111|6|Mentioned|p38|||||||||
19954|Whypalla Supersuite|43285|5|Briefly described|Map Legend||Early Permian|||||||
19954|Whypalla Supersuite|43625|4|Described|p52|Early Triassic|Late Permian|Age: 275-285 Ma||||||
19954|Whypalla Supersuite|44246|6|Mentioned|Map Legend||Early Permian|||||||
19954|Whypalla Supersuite|50335|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province||||||
19954|Whypalla Supersuite|50387|5|Briefly described|Map legend|Permian|Permian|Geological Province: Kennedy Province.||||||
19954|Whypalla Supersuite|50596|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Mount Pike Granite, Bullhead Granite.||||||
19954|Whypalla Supersuite|50630|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Mount Pike Granite.||||||
19954|Whypalla Supersuite|60425|3|Fully described|p11, p56 Tb. 4, p80, p274-7 Appdx. 1|Early Permian|Early Permian|Contains 16 named granites in 6 named Suites. Intruded Hodgkinson Formation. Age: 282+/-9Ma (Rb-Sr). Extensively deformed rocks, S-type granites. Geological province: Hodgkinson Province. Very detailed lithology included.||||||07-FEB-11
19954|Whypalla Supersuite|61527|5|Briefly described|p790 Fig.1|||Includes the Desailley Granite. See also p796.||||||30-JAN-06
19954|Whypalla Supersuite|62371|5|Briefly described|p472 Fig.3|Permian|Permian|S-type granite.||||||
19954|Whypalla Supersuite|63140|6|Mentioned|p572 fig 3|Early Permian|Early Permian||||||S-type.|
19954|Whypalla Supersuite|63154|5|Briefly described|p281 Fig. 3|Late Carboniferous|Late Carboniferous|Geological province: Hodgkinson Province. Granites are S-type.||||||
19954|Whypalla Supersuite|66852|5|Briefly described|pp937-938, p941.|||Most areally extensive suite of granites in Hodgkinson Province. The geometry of its plutons has been influenced by the WNW-ESE Desailly Structure, described in the article.|c.285 - c.265 Ma (Bultitude & Champion 1992).||Includes Nangee, Koobaba, Cannibal Creek, Mount Pike/Bullhead, Kelly St George, Desailly Granites.||Extensive suite of granites.|
19954|Whypalla Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Brodies Camp, Woodstock and Yates Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
19954|Whypalla Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|274.8 +/- 5.1 Ma (SHRIMP).||||S-type granitoids.|
19954|Whypalla Supersuite|69079|6|Mentioned|p24, p42, p45|||Syn-deformation granites. Considered to be an integral part of the major gold mineralising event in the Hodgkinson Province.||||||
19954|Whypalla Supersuite|69582|5|Briefly described|p70|Permian|Carboniferous|Hodgkinson Province. Intrusives of this unit have high heat production (details provided). Atributed to the Kennedy Igneous Association.|285-265 Ma|||Intrudes the Hodgkinson Formation.|Voluminous S-type granitic rocks with moderate to high concentrations of U, Th and K.|
19954|Whypalla Supersuite|69592|6|Mentioned|p247|Permian|Permian|Mentioned in relation to deformation textures (foliations) in surrounding units.||||||
19954|Whypalla Supersuite|69593|3|Fully described|p478-480, p481 Fig.6.4 (b.c), p482|Permian|Permian|See also p505-506, p511. Daintree Subprovince, Kennedy Igneous Association. Comprises the western belt of S-type magmatism in the W, Central and S Hodgkinson Province. Crops out over ~1800 km2. Associated with tungsten deposits (Mount Carbine, Watershed). Enclaves of (garnet) biotite gneiss, "microdiorite", "microgranite", quartz, and locally-derived metasedimentary rocks widespread and locally common. Geochemistry briefly described. Early Permian; younger ages are apparently reset during the Hunter-Bowen Orogeny.|~285-265 Ma.||Cannibal Creek, Curraghmore, Mareeba, Mount Carbine, Mount Pike, Whypalla Suites.||S-type. Highly-porphyritic to even-grained, muscovite-biotite granite; widespread accessory garnet and tourmaline; rare sillimanite, orthopyroxene; plagioclase mostly >K-feldspar.|
19954|Whypalla Supersuite|72297|6|Mentioned|p761|||High heat producing intrusives have potential for geothermal energy.||||||
19954|Whypalla Supersuite|72983|6|Mentioned|p3, p25, p31|Roadian|Kungurian|Granite from this supersuite have U-Pb zircon (SHRIMP) ages ranging from ~270 Ma to ~280 Ma. eNd values range from -4.1 to -6.1. Older than the Cooktown Supersuite by 15-20 Myrs.|~270 Ma to 280 Ma||||S-type granites.|
19954|Whypalla Supersuite|73197|6|Mentioned|p475 Fig.6|Guadalupian|Cisuralian|S-type.|275-268 Ma||||Granitic intrusives.|
20003|Wigton Granite|24382|5|Briefly described|Map legend|Permian|Permian|||||||
20003|Wigton Granite|41738|6|Mentioned|p166|||||||||
20003|Wigton Granite|41778|6|Mentioned|p376|||||||||
20003|Wigton Granite|43008|5|Briefly described|map legend|||||||||
20003|Wigton Granite|43017|5|Briefly described|Fig.3,p375|||||||||
20003|Wigton Granite|63821|5|Briefly described|p27-28|Late Permian|Early Permian|Ages: 255+/-5Ma and 253+/-5Ma (K-Ar biotite), and 262Ma (Rb-Sr biotite). Intrudes Curtis Island Group. Comprises biotite-granite (locally granophyric), hornblende-biotite granodiorite and hornblende-biotite tonalite.||||||07-FEB-11
20003|Wigton Granite|64398|5|Briefly described|Map legend|Late Permian|Late Permian|Biotite granite, K-feldspar-phyric biotite (rapakivi) granite.||||||
20003|Wigton Granite|67874|6|Mentioned|p35|Permian|Permian|Mentioned as possible source of 272.2 +/- 2.6 Ma inherited zircons in Aranbanga Volcanic Group.||||||
20003|Wigton Granite|68679|5|Briefly described|p410, p420-421, p429, p439|||Ellis (1968); Stenson (1997). The most extensive unit in the southern Gayndah-Gladstone belt; covers ~366 km2. Crops out on the NW margin of the Esk Basin. Much of southern part of this unit is now the Hivesville Granite; some other parts are now the Canoe Creek Granite. Several age determinations in this age range given.|282-253 Ma.|||Is overlain by Abernethy Basalt (Aranbanga Volcanic Group).|Two calc-alkaline, medium-K, metaluminous to peraluminous granodiorite plutons; one is I-type. In the north, biotite granite (locally granophyric), hornblende-biotite granodiorite and hornblende-biotite tonalite; rapakivi, biotite granite.|
20003|Wigton Granite|73197|6|Mentioned|p476 Fig.7, p479|Middle Triassic|Lopingian|New England Orogen, northern, Hunter-Bowen Orogenic phase. Partly S-type intrusives.|~255-245 Ma||||Intrusives.|
20009|Wild Cattle Trachyte Member|39969|6|Mentioned|p9|||||||||
20009|Wild Cattle Trachyte Member|73450|6|Mentioned|p92|||Of Stevens, 1965; Grenfell, 1984; Ewart & Grenfell, 1985. Never described in detail.||Governors Chair Volcanics|||Felsic.|29-SEP-22
20012|Wild Granite|23503|5|Briefly described|Map Legend||Late Carboniferous|of O'Briens Creek Supersuite. Age: 315 +/- 8Ma, Rb-Sr.||||||
20012|Wild Granite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Intrusive No. 299. I-Type.||||||
20012|Wild Granite|23616|5|Briefly described|p100 Appendix 2||Carboniferous|Of O'Briens Creek Supersuite.||||||02-JUN-09
20012|Wild Granite|40743|6|Mentioned|Fig.2|||||||||
20012|Wild Granite|41824|6|Mentioned|p201|||||||||
20012|Wild Granite|60425|4|Described|p286-7 Appdx. |Late Carboniferous|Late Carboniferous|Of Nettle Suite (O'Briens Creek Supersuite). Includes Stinking Cornishman Microgranite on most recent maps. Ages: 308+/-4Ma, 311Ma, 313Ma, 315+/-8Ma (Rb-Sr). White, coarse-grained biotite granite. I-type.||||||07-FEB-11
20012|Wild Granite|69593|5|Briefly described|p510|||Herberton and Tate Subprovinces, Kennedy Igneous Association. Sm-Nd isotope data tabulated.|300 Ma.|O'Briens Creek Supersuite.||||
20031|Wilgunya Subgroup|13516|5|Briefly described|p167 fig 10,  p169 fig 11|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
20031|Wilgunya Subgroup|23496|6|Mentioned|p59|||||||||
20031|Wilgunya Subgroup|29591|6|Mentioned|p69|||||||||
20031|Wilgunya Subgroup|31168|5|Briefly described|p11|||See also Table 2.||||||
20031|Wilgunya Subgroup|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
20031|Wilgunya Subgroup|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|39445|6|Mentioned|Table 11|||||||||
20031|Wilgunya Subgroup|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|41307|6|Mentioned|p17|||||||||
20031|Wilgunya Subgroup|43110|5|Briefly described|p55|||||||||
20031|Wilgunya Subgroup|43630|6|Mentioned|p70|||||||||
20031|Wilgunya Subgroup|63979|6|Mentioned|p48|||Of the Rolling Downs Group. Superseded Wilgunya Formation. Lower part comprises Wallumbilla Formation.||||||07-FEB-11
20031|Wilgunya Subgroup|66623|6|Mentioned|p258.|||Laterally equivalent to Wallumbilla Formation in NSW.||Unit in Rolling Downs Group (QLD).||||06-JUN-13
20031|Wilgunya Subgroup|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cretaceous|Early Cretaceous|Eromanga/Carpentaria Basins|||||Fossiliferous mudstone, minor labile, glauconitic and quartzose sandstone, calcareous concretions common|
20031|Wilgunya Subgroup|67784|5|Briefly described|p26|Aptian|Barremian|Carpentaria, Eromanga Basins.|||Gilbert River, Wallumbilla, Toolebuc, Allaru, Normanton FZs.|||
20031|Wilgunya Subgroup|69457|5|Briefly described|p41:2-4, 6-11, 14|Early Cretaceous|Early Cretaceous|Casey (1959); Australian Water Resources Council (1975). Eromanga Basin. This Subgroup's nomenclature is more appropriate (than the Marree Subgroup) in the NT, where the Coorikiana Sandstone has not been recognised.||Rolling Downs Group.|Wallumbilla, Toolebuc Formations; Allaru Mudstone.|Is overlain by Manuka Subgroup. Equivalent to Marree Subgroup.||12-JUL-16
20031|Wilgunya Subgroup|69458|6|Mentioned|p42:16|||Eromanga Basin. Some rocks of this unit are mapped as Rumbalara Shale in HALE RIVER, McDILLS map areas.||||Is overlain unconformably by Etingambra Formation.||12-JUL-16
20031|Wilgunya Subgroup|69594|5|Briefly described|p528|||Great Australian Superbasin.||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|69599|5|Briefly described|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by the Noranside Limestone.||
20031|Wilgunya Subgroup|69673|6|Mentioned|p156|||||Rolling Downs Group|Includes Wallumbilla Formation, Toolebuc Formation, Allaru Mudstone|Overlain by Manuka Subgroup||
20031|Wilgunya Subgroup|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group|Includes Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|||20-JAN-22
20031|Wilgunya Subgroup|73083|6|Mentioned|p62, p65, p77|||Term used where the Wallumbilla Mudstone and Allaru Mudstone are indistinguishable. [Written as Wilgunyah Subgroup on p65 and p77].||||||
20083|Williams Granite|9830|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Coarse porphyritic granite.||||||27-AUG-04
20083|Williams Granite|22522|6|Mentioned|Fig2p332,Fig3p333|||||||||
20083|Williams Granite|23068|5|Briefly described|p784 (Fig 1)|||||||||
20083|Williams Granite|23966|5|Briefly described|p1309 Fig. 2|Proterozoic|Proterozoic|Geological Province: Mount Isa Inlier.||||||
20083|Williams Granite|23967|6|Mentioned|p1331 Fig.1|||||||||
20083|Williams Granite|24168|6|Mentioned|p635|||||||||
20083|Williams Granite|24567|5|Briefly described|p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: ca1500Ma. Geological Province: Mount Isa Inlier. Name written as Williams only under heading for GRANITE.||||||09-MAY-05
20083|Williams Granite|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20083|Williams Granite|31043|6|Mentioned|p57|||||||||
20083|Williams Granite|31867|6|Mentioned|p25|||||||||
20083|Williams Granite|32660|5|Briefly described|Table 5|||||||||
20083|Williams Granite|32959|6|Mentioned|Fig.21|||||||||
20083|Williams Granite|33900|6|Mentioned|p15|||||||||
20083|Williams Granite|35074|6|Mentioned|Fig.2|||||||||
20083|Williams Granite|35139|6|Mentioned|p10|||||||||
20083|Williams Granite|35295|6|Mentioned|p601|||Also mention p602.||||||01-FEB-07
20083|Williams Granite|37462|4|Described|Table4.VII|||||||||
20083|Williams Granite|37862|6|Mentioned|p587|||||||||
20083|Williams Granite|38275|6|Mentioned|p183|||||||||
20083|Williams Granite|39043|6|Mentioned|p9|||||||||
20083|Williams Granite|39445|6|Mentioned|p43|||See also Table 2. Disused||||||
20083|Williams Granite|39496|6|Mentioned|p14|||||||||
20083|Williams Granite|41306|6|Mentioned|p4|||||||||
20083|Williams Granite|41464|6|Mentioned|Map legend|Proterozoic||||||||
20083|Williams Granite|41556|6|Mentioned|Map legend|Proterozoic||||||||
20083|Williams Granite|41568|4|Described|p15|||||||||
20083|Williams Granite|41744|6|Mentioned|Fig.1|||||||||
20083|Williams Granite|41761|6|Mentioned|Fig.1|||||||||
20083|Williams Granite|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Granite, generally non-foliated.||||||09-FEB-09
20083|Williams Granite|44271|2|Defined|p37,38,46,48||Paleoproterozoic|||||||07-NOV-08
20083|Williams Granite|44275|14|Not recorded|Map Legend|||||||||
20083|Williams Granite|44276|2|Defined|p13-15,17,map|||||||||
20083|Williams Granite|44751|14|Not recorded|p300||Precambrian|||||||
20083|Williams Granite|44788|14|Not recorded|p29|||||||||
20083|Williams Granite|44849|14|Not recorded|p74|||||||||
20083|Williams Granite|44989|2|Defined|p.148-9|||On many pages. (F54-6).||||||
20083|Williams Granite|45003|14|Not recorded|p30|||||||||
20083|Williams Granite|45161|6|Mentioned|p51|||A series of granitic plutons referred to as Williams Batholith.||||||01-FEB-07
20083|Williams Granite|45166|5|Briefly described|p77|||||||||
20083|Williams Granite|45287|14|Not recorded|p.227,228|||||||||
20083|Williams Granite|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
20083|Williams Granite|48906|14|Not recorded|p4,12,14,27,28,Pl.6|||||||||
20083|Williams Granite|48908|6|Mentioned|p25||Precambrian|||||||
20083|Williams Granite|49009|6|Mentioned|p6|||||||||
20083|Williams Granite|50100|5|Briefly described|p21|Calymmian|Calymmian|Of the Williams Supersuite.||||||
20083|Williams Granite|50332|5|Briefly described|p22|Mesoproterozoic|Mesoproterozoic|Of the Williams and Naraku Batholiths. Age: 1520-1450Ma. Geological Province: Quamby-Malbon and Cloncurry Subprovinces.||||||17-APR-12
20083|Williams Granite|60665|6|Mentioned|p1146|Calymmian|Calymmian|Postmetamorphic.|1550-1500 Ma.|Unit in Williams Suite.||||
20083|Williams Granite|61925|5|Briefly described|p56 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
20083|Williams Granite|61926|5|Briefly described|p71 Fig. 1|||Geological Province: Eastern Fold Belt, Mount Isa Inlier.||||||
20083|Williams Granite|63055|5|Briefly described|p12 Fig. 1|||Intrusive rocks of the Williams Batholith - together with Naraku Granite.||||||
20083|Williams Granite|63593|5|Briefly described|p283, p285 Fig.1,p287, p288 Fig.2.|Mesoproterozoic|Mesoproterozoic|See also p289, p291, p293, p296-297. Also referred to in the article as Williams-Naraku granites (p283, 296, 298), Williams/Narabu [sic] Granite (in Fig.1), Williams and Naraku batholiths (p287), Williams and Naraku Granite (Fig.2), Williams-Naraku batholith (p289). Whichever name one picks, the authors suggest that fluids from these intrusions caused fluid over-pressuring, leading to extensive brecciation and related mineralization.|ca. 1500 Ma|||||
20083|Williams Granite|65396|6|Mentioned|p53 Fig.1, p157|||Eastern Succession.||Williams Supersuite||||
20083|Williams Granite|67323|6|Mentioned|p72|||Contains a Zn anomaly and minor IOGC anomalies.||||||
20083|Williams Granite|68732|6|Mentioned|p158 Fig.1|||Mount Isa Inlier.||||||
20083|Williams Granite|69056|5|Briefly described|p14 Tb.3, p18, p23, p28|||Includes Mount Margaret Granite for modelling purposes. Two variations are also presented: High Mag and Low Mag for their respective magnetic susceptibilities. Modelling values listed.||Williams Supersuite.||||
20124|Wills Creek Granite|24197|5|Briefly described|p21, p94 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Of the Kalkadoon Supersuite. Age: 1860Ma. Geological province: Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
20124|Wills Creek Granite|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20124|Wills Creek Granite|37862|4|Described|p584|||||||||
20124|Wills Creek Granite|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20124|Wills Creek Granite|38900|6|Mentioned|p55|||||||||
20124|Wills Creek Granite|39445|5|Briefly described|Table 2|||||||||
20124|Wills Creek Granite|40840|6|Mentioned|Map legend|||||||||
20124|Wills Creek Granite|45161|4|Described|p29|||||||||
20124|Wills Creek Granite|45166|6|Mentioned|p11|||||||||
20124|Wills Creek Granite|46962|6|Mentioned|p249|||||||||
20124|Wills Creek Granite|49009|2|Defined|p49|Proterozoic|Proterozoic|Mapped as Argylla Formation and Kalkadoon Group(Carter and Opik, 1963).||||||19-DEC-06
20124|Wills Creek Granite|49041|5|Briefly described|Table 2|||||||||
20124|Wills Creek Granite|50100|5|Briefly described|p16|Proterozoic|Proterozoic|Of the Kalkadoon Batholith.  Min. age: 1830Ma (Wyborn and Page, 1983).||||||
20124|Wills Creek Granite|50536|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Kalkadoon Suite.||||||07-NOV-08
20124|Wills Creek Granite|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Medium to coarse leucocratic biotite granite.||||||
20124|Wills Creek Granite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map., p14|Paleoproterozoic|Paleoproterozoic|Kalkadoon Igneous Event. Kalkadoon-Leichhardt Domain, central Mount Isa Block.||Kalkadoon Suite or Supersuite|||Medium to coarse biotite granite and leucogranite; minor aplite.|
20124|Wills Creek Granite|69591|5|Briefly described|p31, p60|||Kalkadoon Batholith, Kalkadoon-Leichhardt Domain, Mount Isa Province.||Kalkadoon Suite.|||Medium to coarse biotite granite and leucogranite; minor aplite.|
20124|Wills Creek Granite|73553|6|Mentioned|p6, p8 Fig.1.2.3|||Kalkadoon-Leichhardt Domain.||Kalkadoon Suite||||
20253|Winnathoola Coal Member|24069|5|Briefly described|p283 Fig. 3|Permian|Permian|Of Black Alley Shale. Geological Province: Surat Basin.||||||
20253|Winnathoola Coal Member|32578|2|Defined|p352|Late Permian|Late Permian|See also P345, P347, P348, P349, P350 etc.. In Black Alley Shale||||||
20253|Winnathoola Coal Member|36739|6|Mentioned|p22|||||||||
20253|Winnathoola Coal Member|45110|6|Mentioned|Table 16|||Misspelling of Tinowon ? [not even in Tinowon Formation - see 79/03361 - APL 06/1995]||||||
20253|Winnathoola Coal Member|63713|5|Briefly described|p1507 Fig.2, p1528|Capitanian|Capitanian|Roma Shelf, Bowen Basin. Appears [ambiguously] as Winnathoola CM and [perhaps unsurprisingly] as Winnathoola Coal Measures on p1528. Well-log correlation.||Unit in Black Alley Shale.||||
20253|Winnathoola Coal Member|64856|4|Described|p65-67|Late Permian|Late Permian|Paten and Groves (1974). Coal Member of Black Alley Shale. Black to brown coal, dull with minor pyrite; associated sandstone; minor calcareous cement.|| ||||29-NOV-17
20253|Winnathoola Coal Member|64858|5|Briefly described|p182|Late Permian|Late Permian|Member of the Black Alley Shale.||||||30-NOV-09
20253|Winnathoola Coal Member|67669|5|Briefly described|p11|Late Permian|Late Permian|Of Bowen Basin.||||Overlain by Bandanna Formation. Equivalent to Black Alley Shale or Fort Copper or Gyranda Coal Measures.||
20268|Winton Formation|12597|5|Briefly described|p492 Tb.1, p500, p501|Cenomanian|Cenomanian|Eromanga Basin. 400-700m, locally up to 1200m, thick.||||Overlies Mackunda Formation.|Basal paralic-nonmarine transition zone, overlain by non-marine sequence of fine- to medium-grained labile sandstone, siltstone, mudstone and lenticular coal seams.|
20268|Winton Formation|13497|5|Briefly described|p13, p115, p115 fig 6.33|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposited in a high-sinuosity fluvial environment. See also p144, p144 fig 9.2, p146, p148-p154, .||||Overlies the Mackunda Formation and the Oodnadatta Formation. Unconformably overlain by the Mount Howie Sandstone and the Eyre Formation.|Sandstone, siltstone, shale and coal.|
20268|Winton Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
20268|Winton Formation|22464|6|Mentioned|p9||Late Cretaceous|Also p8. In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22587|5|Briefly described|p71|Cenomanian|Albian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22773|6|Mentioned|p338|||||||||
20268|Winton Formation|22839|6|Mentioned|P33|||||||||
20268|Winton Formation|22857|4|Described|p296-7 Tb 22.1, p326, p552 Tb A1.13|Cenomainian|Cenomainian|Of the Rolling Downs Group. Interbedded mudstone and lithic and feldspathic arenite. Max. thickness: 400m in NSW. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
20268|Winton Formation|22862|6|Mentioned|p327||Cenomanian|||||||
20268|Winton Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Cenomanian|||||||
20268|Winton Formation|22883|5|Briefly described|P31, Fig2||Late Cretaceous|Underlying unit is Mackunda Formation.||||||19-DEC-06
20268|Winton Formation|22912|6|Mentioned|34|||Geological province: Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23054|6|Mentioned|Fig5p22|||||||||
20268|Winton Formation|23056|6|Mentioned|9|||Geol province Eromanga Basin. Parent Rolling Downs Group||||||
20268|Winton Formation|23154|5|Briefly described|Map Legend|Late Cretaceous|Late Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|23155|4|Described|p33|Late Cretaceous|Early Cretaceous|Uppermost Eromanga Basin unit known on STRZELECKI, and is disconformably overlain by Tertiary Eyre Formation.||||||19-DEC-06
20268|Winton Formation|23375|5|Briefly described|Fig2 p265||Cenomanian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
20268|Winton Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66|Cenomanian|Cenomanian|Geological Province: Cooper Basin. Of the Manuka Sub-Group. Max. thickness: >2000 ft.||||||18-APR-05
20268|Winton Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
20268|Winton Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
20268|Winton Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Rolling Downs Group.||||||
20268|Winton Formation|23916|5|Briefly described|p523|Cenomanian|Albian|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24112|5|Briefly described|p270|Cenomanian|Albian|Age: 97-90Ma (Krieg et al, 1995). Geological Province: Eromanga Basin||||||
20268|Winton Formation|24175|3|Fully described|p30, p17 Fig. 3|Cenomanian|Albian|Overlain by Eyre Formation; conformably overlies Mackunda Formation.  Max. thickness: 88m.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24204|5|Briefly described|p263 Fig.4, p267|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
20268|Winton Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
20268|Winton Formation|24251|5|Briefly described|p234 Fig.1|Cenomanian|Cenomanian|Geological Province: Eromanga Basin||||||
20268|Winton Formation|24321|5|Briefly described|Map legend|Cenomanian|Cenomanian|Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|29591|6|Mentioned|p71|||||||||
20268|Winton Formation|29721|6|Mentioned|Table 137|||||||||
20268|Winton Formation|30019|6|Mentioned|p2|||||||||
20268|Winton Formation|30055|6|Mentioned|p159|||||||||
20268|Winton Formation|30102|6|Mentioned|Table 4|||See also p36,37.||||||19-DEC-06
20268|Winton Formation|30104|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper? Cretaceous||||||
20268|Winton Formation|30514|6|Mentioned|p102|||Middle Cretaceous age.||||||
20268|Winton Formation|30539|6|Mentioned|p7|||Late Albian - early Cenomanian age||||||
20268|Winton Formation|30540|6|Mentioned|Fig.6|||||||||
20268|Winton Formation|30691|4|Described|p17|||See also p21,Table 4. Lower - Upper Cretaceous||||||19-DEC-06
20268|Winton Formation|30700|6|Mentioned|p28|||||||||
20268|Winton Formation|30803|6|Mentioned|p2|||Cretaceous age||||||
20268|Winton Formation|30804|6|Mentioned|p7|||On Table 1. See also Table 2.||||||
20268|Winton Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
20268|Winton Formation|30853|5|Briefly described|Table 3|||Lower to Upper Cretaceous||||||
20268|Winton Formation|30854|4|Described|Table 4|||Lower to Upper Cretaceous age.||||||19-DEC-06
20268|Winton Formation|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|Unit in Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|30856|4|Described|Table 3|||On p10. Lower-Upper Cretaceous.||||||19-DEC-06
20268|Winton Formation|30857|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|30918|6|Mentioned|p82|||||||||
20268|Winton Formation|30919|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20268|Winton Formation|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|L. - U. Cretaceous||||||
20268|Winton Formation|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
20268|Winton Formation|31425|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower-Upper? Cretaceous||||||
20268|Winton Formation|31430|5|Briefly described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
20268|Winton Formation|31432|4|Described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31438|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|31553|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31649|6|Mentioned|p63|||||||||
20268|Winton Formation|31699|4|Described|p133|||Middle Cretaceous||||||
20268|Winton Formation|31706|6|Mentioned|p669|||Cretaceous correlation chart||||||
20268|Winton Formation|31923|6|Mentioned|p15|||||||||
20268|Winton Formation|32274|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|32275|6|Mentioned|p6|||||||||
20268|Winton Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
20268|Winton Formation|32314|6|Mentioned|Fig. 4|||||||||
20268|Winton Formation|32396|6|Mentioned|p10|||Equivalents||||||
20268|Winton Formation|32413|6|Mentioned|p103|||||||||
20268|Winton Formation|32472|6|Mentioned|p17|||||||||
20268|Winton Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
20268|Winton Formation|32696|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|32796|6|Mentioned|p303|||||||||
20268|Winton Formation|32918|6|Mentioned|p20|||||||||
20268|Winton Formation|33016|6|Mentioned|p1|||Table on P1||||||
20268|Winton Formation|33017|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33067|4|Described|Table 1|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
20268|Winton Formation|33069|4|Described|p7|||||||||
20268|Winton Formation|33072|4|Described|Table 1|||L.Cret.||||||
20268|Winton Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|33075|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
20268|Winton Formation|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33081|6|Mentioned|p26|||||||||
20268|Winton Formation|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33087|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|33089|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33095|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
20268|Winton Formation|33368|6|Mentioned|p25|||Strat.Table.||||||
20268|Winton Formation|33372|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33414|6|Mentioned|p212-214,Tb.||Cenomanian|Part of Manuka Sub-Group.||||||
20268|Winton Formation|33448|4|Described|Table 1|||L.-U.Cret.||||||11-JAN-10
20268|Winton Formation|33449|4|Described|Table 1|||L.-U.Cret.||||||
20268|Winton Formation|33452|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33490|6|Mentioned|p30|||Cret. sediments. Correlation||||||
20268|Winton Formation|33521|6|Mentioned|p10|||Upper Cretaceous||||||
20268|Winton Formation|33561|6|Mentioned|p102|||||||||
20268|Winton Formation|33569|6|Mentioned|p63|||||||||
20268|Winton Formation|33639|5|Briefly described|p12|||L.-U.Cret.||||||
20268|Winton Formation|33640|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33642|6|Mentioned|p144-45,147,148,Tb.1|||Refers Dunstan (1916) & Whitehouse (1954)||||||
20268|Winton Formation|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Creataceous||||||
20268|Winton Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
20268|Winton Formation|33819|6|Mentioned|p1|||||||||
20268|Winton Formation|33820|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|33822|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33824|6|Mentioned|p7|||P12, Tables 1 & 2||||||
20268|Winton Formation|33825|6|Mentioned|p8|||Strat. table. Lithology||||||
20268|Winton Formation|33827|6|Mentioned|p7|||See also p3 and Tables 1 and 3.||||||19-DEC-06
20268|Winton Formation|33828|6|Mentioned|p9|||See also Table 1||||||
20268|Winton Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33832|6|Mentioned|p6|||Strat.||||||
20268|Winton Formation|33936|6|Mentioned|Fig.3A|||Cret.||||||
20268|Winton Formation|33937|6|Mentioned|p3|||||||||
20268|Winton Formation|33938|6|Mentioned|p19|||Refers Jack (1930).||||||
20268|Winton Formation|33964|4|Described|p6|||||||||
20268|Winton Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
20268|Winton Formation|34035|6|Mentioned|p544|||Cret.||||||
20268|Winton Formation|34061|6|Mentioned|p53|||||||||
20268|Winton Formation|34065|4|Described|p6|||L.-U. Cret.||||||
20268|Winton Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|34218|4|Described|Table 1|||Lower - Upper Cretaceous. See also pp8,10-12 etc.||||||19-DEC-06
20268|Winton Formation|34254|6|Mentioned|p492|||||||||
20268|Winton Formation|34259|6|Mentioned|p451|||||||||
20268|Winton Formation|34282|6|Mentioned|p88|||See also PP90, 93 etc.||||||
20268|Winton Formation|34287|6|Mentioned|p199|||Cret.||||||
20268|Winton Formation|34356|6|Mentioned|p32|||||||||
20268|Winton Formation|34400|6|Mentioned|p14|||Lower Cretaceous||||||
20268|Winton Formation|34454|5|Briefly described|Table 1|||Cretaceous. See also pp6,12,15.||||||19-DEC-06
20268|Winton Formation|34485|5|Briefly described|Table 1|||Lower - Upper? Cretaceous.||||||19-DEC-06
20268|Winton Formation|34486|5|Briefly described|Table 1|||Lower - Upper? Cretaceous. See also Table 2||||||
20268|Winton Formation|34487|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34543|6|Mentioned|p98|||||||||
20268|Winton Formation|34611|4|Described|p158|||Cretaceous. See Fig.65,66||||||
20268|Winton Formation|34909|6|Mentioned|p992|||||||||
20268|Winton Formation|34948|6|Mentioned|Fig. 70|||||||||
20268|Winton Formation|35067|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|35139|6|Mentioned|p17|||||||||
20268|Winton Formation|35151|6|Mentioned|p147|||||||||
20268|Winton Formation|35239|6|Mentioned|p258|||||||||
20268|Winton Formation|35560|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|35793|4|Described|p241|||Details of weathering and profiles.||||||
20268|Winton Formation|35811|5|Briefly described|Table 3|||||||||
20268|Winton Formation|35894|6|Mentioned|p275|||||||||
20268|Winton Formation|36172|6|Mentioned|Appendix|||||||||
20268|Winton Formation|36213|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|36229|6|Mentioned|Map legend|Eocene|Eocene|||||||
20268|Winton Formation|36243|6|Mentioned|Table 6A|||||||||
20268|Winton Formation|36327|6|Mentioned|p7|||||||||
20268|Winton Formation|36571|6|Mentioned|p98|||See also Table 4.||||||
20268|Winton Formation|36912|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|36922|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|37065|5|Briefly described|p41|||||||||
20268|Winton Formation|37114|6|Mentioned|p308|||||||||
20268|Winton Formation|37116|4|Described|p312|||||||||
20268|Winton Formation|37261|6|Mentioned|p351|||||||||
20268|Winton Formation|37263|6|Mentioned|p319|||||||||
20268|Winton Formation|37287|6|Mentioned|p36|||||||||
20268|Winton Formation|37451|6|Mentioned|Table 2|||||||||
20268|Winton Formation|37603|6|Mentioned|p444|||||||||
20268|Winton Formation|37607|6|Mentioned|p333|||||||||
20268|Winton Formation|37608|3|Fully described|Table 1|||||||||
20268|Winton Formation|37776|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|38068|5|Briefly described|p72|||||||||
20268|Winton Formation|38226|6|Mentioned|p414|||See also Fig.6.||||||
20268|Winton Formation|38373|6|Mentioned|p622|||||||||
20268|Winton Formation|38779|6|Mentioned|p3|||||||||
20268|Winton Formation|38814|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39070|4|Described|p366|||||||||
20268|Winton Formation|39085|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39211|5|Briefly described|Fig.3, Fig.6|||See also Figs 4,5,7,14,15 etc. Correlation||||||
20268|Winton Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
20268|Winton Formation|39445|5|Briefly described|Table 11|||||||||
20268|Winton Formation|39478|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39482|6|Mentioned|Fig.7|||||||||
20268|Winton Formation|39846|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39847|5|Briefly described|p40|||||||||
20268|Winton Formation|39914|6|Mentioned|p3|||||||||
20268|Winton Formation|39943|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40003|6|Mentioned|Fig.9   or|||||||||
20268|Winton Formation|40058|6|Mentioned|Fig.1|||||||||
20268|Winton Formation|40121|6|Mentioned|Table 1|||||||||
20268|Winton Formation|40150|6|Mentioned|p77|||||||||
20268|Winton Formation|40199|6|Mentioned|p16|||||||||
20268|Winton Formation|40220|6|Mentioned|p7|||||||||
20268|Winton Formation|40249|6|Mentioned|p41|||||||||
20268|Winton Formation|40322|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|40670|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|40675|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40681|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|40756|6|Mentioned|Fig.1.2|||||||||
20268|Winton Formation|40757|6|Mentioned|p78|||Now known to be Eyre Formation||||||
20268|Winton Formation|40801|6|Mentioned|p29|||Mention also Fig.21||||||
20268|Winton Formation|40910|6|Mentioned|p15|||See also P17||||||
20268|Winton Formation|40911|6|Mentioned|Map legend|Cenomanian|Albian|Albian-?Cenomanian||||||
20268|Winton Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|40926|3|Fully described|p18|||||||||
20268|Winton Formation|41057|6|Mentioned|p82|||||||||
20268|Winton Formation|41060|6|Mentioned|p3|||Generalized stratigraphy||||||
20268|Winton Formation|41061|6|Mentioned|p19|||||||||
20268|Winton Formation|41062|6|Mentioned|p35|||||||||
20268|Winton Formation|41063|6|Mentioned|p40|||||||||
20268|Winton Formation|41064|6|Mentioned|p62|||||||||
20268|Winton Formation|41085|6|Mentioned|p90|||||||||
20268|Winton Formation|41086|3|Fully described|p98|||See also Fig.3||||||
20268|Winton Formation|41088|6|Mentioned|p144|||See also Fig.2||||||
20268|Winton Formation|41097|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41098|4|Described|p177|||||||||
20268|Winton Formation|41099|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|41165|5|Briefly described|p363|||See also Fig.15.||||||19-DEC-06
20268|Winton Formation|41174|6|Mentioned|p117|||||||||
20268|Winton Formation|41176|6|Mentioned|p206|||See also P211||||||
20268|Winton Formation|41177|6|Mentioned|p233|||||||||
20268|Winton Formation|41182|5|Briefly described|Fig.2|||||||||
20268|Winton Formation|41183|4|Described|p307|||||||||
20268|Winton Formation|41184|6|Mentioned|p346|||||||||
20268|Winton Formation|41187|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|41198|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41214|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41216|6|Mentioned|p299|||||||||
20268|Winton Formation|41219|6|Mentioned|p338|||||||||
20268|Winton Formation|41266|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41523|3|Fully described|p282|||See also p283.||||||19-DEC-06
20268|Winton Formation|41535|6|Mentioned|p369|||||||||
20268|Winton Formation|41707|6|Mentioned|Fig.8|||||||||
20268|Winton Formation|41720|6|Mentioned|p372|||||||||
20268|Winton Formation|41724|5|Briefly described|p383|||||||||
20268|Winton Formation|41950|5|Briefly described|Fig.2 P3|||||||||
20268|Winton Formation|42061|4|Described|Fig,11 P159|||See also Fig.11||||||
20268|Winton Formation|42067|6|Mentioned|Fig.2 P309|||||||||
20268|Winton Formation|42071|6|Mentioned|p117|||||||||
20268|Winton Formation|42084|6|Mentioned|Fig.3 P256|||||||||
20268|Winton Formation|42085|6|Mentioned|Fig.2 P374|||||||||
20268|Winton Formation|42187|6|Mentioned|Fig.5 P322|||||||||
20268|Winton Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
20268|Winton Formation|42346|5|Briefly described|p84|Cretaceous||||||||
20268|Winton Formation|42375|6|Mentioned|p30, p121, p125|Late Cretaceous|Jurassic|Eromanga Basin.||||||
20268|Winton Formation|42395|5|Briefly described|Fig.13 P83|||||||||
20268|Winton Formation|42397|6|Mentioned|Fig.2 P3|||||||||
20268|Winton Formation|42429|5|Briefly described|p155|Cenomanian||||||||
20268|Winton Formation|42447|6|Mentioned|Fig. 1|||||||||
20268|Winton Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
20268|Winton Formation|42520|5|Briefly described|p6|||||||||
20268|Winton Formation|42543|5|Briefly described|Fig.4 P6|||||||||
20268|Winton Formation|42645|6|Mentioned|p195|||||||||
20268|Winton Formation|42648|5|Briefly described|Fig.7 P43|||||||||
20268|Winton Formation|42673|5|Briefly described|Fig.2, P184|||||||||
20268|Winton Formation|42746|4|Described|p12|||See also Fig.2, Fig.6||||||
20268|Winton Formation|42749|6|Mentioned|Fig.2 P27|||||||||
20268|Winton Formation|42784|6|Mentioned|p492|||||||||
20268|Winton Formation|42905|5|Briefly described|p20, Fig 5.3|||||||||
20268|Winton Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
20268|Winton Formation|43002|5|Briefly described|Fig.2,p135|||||||||
20268|Winton Formation|43004|5|Briefly described|Table 1,p179|||||||||
20268|Winton Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolaustrine mudstone and siltstone.||||||25-MAY-05
20268|Winton Formation|43085|5|Briefly described|Fig.3|||||||||
20268|Winton Formation|43105|6|Mentioned|p15|||||||||
20268|Winton Formation|43114|6|Mentioned|Table 2|||||||||
20268|Winton Formation|43122|5|Briefly described|Fig.2.|||||||||
20268|Winton Formation|43252|5|Briefly described|p163|||||||||
20268|Winton Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43344|14|Not recorded|p14|||||||||
20268|Winton Formation|43383|14|Not recorded|p27|||||||||
20268|Winton Formation|43384|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|43390|14|Not recorded|p16|||Part of Rolling Downs Group||||||
20268|Winton Formation|43452|14|Not recorded|Map Legend||Cretaceous|Of the Rolling Downs Group.||||||14-FEB-05
20268|Winton Formation|43459|14|Not recorded|p315|||||||||
20268|Winton Formation|43591|6|Mentioned|p40|||||||||
20268|Winton Formation|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
20268|Winton Formation|43628|6|Mentioned|Fig.3|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
20268|Winton Formation|43985|14|Not recorded|7-10,12,Fig.3,Pl.1,2|||||||||
20268|Winton Formation|43995|14|Not recorded|Tb.p9,30,57-8,Fig.3||Late Cretaceous|Fig.15||||||
20268|Winton Formation|44016|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44017|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44018|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44019|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44020|14|Not recorded|p8,10-11,13-15,Tb.1,|Late Cretaceous|Early Cretaceous|Of Rolling Downs Group. Tb.2,3, Fig.3,||||||
20268|Winton Formation|44031|14|Not recorded|p5,6,8,9||Cretaceous|||||||
20268|Winton Formation|44033|4|Described|map,4,8,9,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
20268|Winton Formation|44040|14|Not recorded|p35|||||||||
20268|Winton Formation|44041|6|Mentioned|p251|||||||||
20268|Winton Formation|44066|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44067|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44068|14|Not recorded|p17,18|||||||||
20268|Winton Formation|44082|14|Not recorded|p28,30,Tb.p34|||||||||
20268|Winton Formation|44087|14|Not recorded|p4,8-12|||Lacustrine.||||||
20268|Winton Formation|44088|14|Not recorded|Tb.1,opp.p6,7,8,map|||||||||
20268|Winton Formation|44089|4|Described|p3-6,8-10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44090|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44091|14|Not recorded|p61||Cretaceous|||||||
20268|Winton Formation|44098|14|Not recorded|p98|||||||||
20268|Winton Formation|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|(Rolling Downs Group)||||||
20268|Winton Formation|44115|14|Not recorded|p17,20|||||||||
20268|Winton Formation|44119|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44120|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44121|14|Not recorded|p5-8,10,12||Cretaceous|See also Lexicon.||||||
20268|Winton Formation|44122|2|Defined|p318-324|||||||||
20268|Winton Formation|44133|4|Described|p123, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Maximum Thickness: ~1200m. Includes part of the now superseded Blanchewater Formation.||||||
20268|Winton Formation|44168|14|Not recorded|Tb.1p5,7,8,10,map|||||||||
20268|Winton Formation|44269|14|Not recorded|p18||Cretaceous|||||||
20268|Winton Formation|44291|14|Not recorded|p5|||||||||
20268|Winton Formation|44310|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44346|14|Not recorded|p4|||||||||
20268|Winton Formation|44374|14|Not recorded|p12||Cretaceous|Freshwater-final withdrawal of sea from Eromanga Basin.||||||
20268|Winton Formation|44375|14|Not recorded|p313|||||||||
20268|Winton Formation|44405|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44406|14|Not recorded|p3-14|Cenomanian|Albian|||||||
20268|Winton Formation|44407|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44408|14|Not recorded|p4,8-13,opp.6|||||||||
20268|Winton Formation|44410|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44413|14|Not recorded|p470,474|||||||||
20268|Winton Formation|44414|14|Not recorded|p110-112||Cretaceous|Mudstone, siltstone and characteristic coal seams.||||||
20268|Winton Formation|44415|14|Not recorded|p22|||||||||
20268|Winton Formation|44417|14|Not recorded|p416,417,420|||||||||
20268|Winton Formation|44418|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44509|14|Not recorded|p342-343|||||||||
20268|Winton Formation|44548|14|Not recorded|p456||Cretaceous|||||||
20268|Winton Formation|44573|14|Not recorded|p98|||||||||
20268|Winton Formation|44611|14|Not recorded|p22,24|||||||||
20268|Winton Formation|44634|14|Not recorded|p29|||||||||
20268|Winton Formation|44715|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
20268|Winton Formation|44807|14|Not recorded|p10|||||||||
20268|Winton Formation|44819|14|Not recorded|p89,90|||Non-marine sandstone, carbonaceous grey shale and coal. No age given.||||||
20268|Winton Formation|44848|14|Not recorded|p99-101|||||||||
20268|Winton Formation|44852|14|Not recorded|p78||Late Cretaceous|||||||
20268|Winton Formation|44915|14|Not recorded|p18,24|||Correlated with upper part of Blanchewater Formation in South Australia. Age not given.||||||
20268|Winton Formation|44998|14|Not recorded|p.169|||||||||
20268|Winton Formation|45004|14|Not recorded|p.8,9|||||||||
20268|Winton Formation|45110|6|Mentioned|Table 18|||||||||
20268|Winton Formation|45168|6|Mentioned|p6|||See also Table 1||||||
20268|Winton Formation|46791|5|Briefly described|p48|||||||||
20268|Winton Formation|46854|6|Mentioned|p241|||||||||
20268|Winton Formation|46911|5|Briefly described|p112|||Analyses of weathered profiles and parent rocks.||||||
20268|Winton Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20268|Winton Formation|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
20268|Winton Formation|48627|14|Not recorded|p3|||||||||
20268|Winton Formation|48634|4|Described|p5,19,20|||See also Fig.2,6,Pl.1,2. Subsidy report. (G54-14).||||||
20268|Winton Formation|48751|6|Mentioned|p19|||||||||
20268|Winton Formation|48906|14|Not recorded|p5,9,Tb.2,Fig.1,Pl.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|48908|14|Not recorded|Tb.1||Late Cretaceous|||||||
20268|Winton Formation|48920|3|Fully described|p62|||Cretaceous age||||||
20268|Winton Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20268|Winton Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|60080|5|Briefly described|Map legend|Late Cretaceous|Early Cretaceous|Very labile sandstone, siltstone and mudstone; calcareous in part, minor mud clast conglomerate.  Overlain by Glendower Formation.||||||22-JUL-04
20268|Winton Formation|60281|6|Mentioned|p11|||||||||
20268|Winton Formation|60331|5|Briefly described|p34 Fig.3||Cenomanian|Overlies Mackunda Formation. Geological Province: Eromanga Basin||||||
20268|Winton Formation|60717|5|Briefly described|p40 Fig. 2|Late Cretaceous|Late Cretaceous|Overlies Oodnadatta Formation and Mackunda Formation. Geological Province: Eromanga Basin. Non-marine to marginal marine deposits.||||||31-JAN-08
20268|Winton Formation|60726|6|Mentioned|p2 Fig.1, p6.|Late Cretaceous|Late Cretaceous|Winton area, Great Artesian Basin.||||||
20268|Winton Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolacustrine mudstone and siltstone.||||||
20268|Winton Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Fluviolacustraine mudstone and siltstone.||||||
20268|Winton Formation|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Consists of interbedded mudstone and lithic and feldspathic sandstone deposited in terrestrial environments. Geological Province: Eromanga Basin (absent in NSW). See also p64, p67 Fig. E5.||||||19-DEC-06
20268|Winton Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
20268|Winton Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
20268|Winton Formation|61823|5|Briefly described|p118|Cenomanian|Late Albian|Predominantly alluvial deposits.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
20268|Winton Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20268|Winton Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
20268|Winton Formation|62376|5|Briefly described|p84|Late Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
20268|Winton Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Mackunda Formation.||
20268|Winton Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
20268|Winton Formation|63979|2|Defined|p54-55, Fig. 44|Cenomanian|Albian|Formerly Winton Series (Dunstan 1916). Forms upper part of Rolling Downs Gp.Conformable on Mackunda Fm; unconformable below Glendower Fm. Max.thick:1000m. Interbedded sands., sandy siltst., siltst., mudst.+ coal with minor intraformational conglomerate.||||||07-FEB-11
20268|Winton Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - lignite. Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|64197|6|Mentioned|p625 Fig.1c, p627, p630 Figs.6,7|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deeply weathered upper surface.||||Overlies Oodnadatta and Mackunda Formations. Is overlain unconformably by Eyre Formation.||11-DEC-15
20268|Winton Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Coal measures are present in this unit and are a potential target for CSM exploration activities.||||||24-JUL-08
20268|Winton Formation|64665|5|Briefly described|p62.|Cretaceous|Cretaceous|Eromanga Basin. Hosts coal seams up to 7 m thick; low rank lignites of no current (i.e. c.2008) commercial interest.||||||
20268|Winton Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
20268|Winton Formation|64856|6|Mentioned|p101|||Eromanga Basin. Younger than lithologically similar Griman Creek Formation in the Surat Basin.|| ||||29-NOV-17
20268|Winton Formation|65238|5|Briefly described|p7 Fig. 8, p10|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Fluvial deposits.||||||
20268|Winton Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 613 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Oodnadatta Shale. Is overlain by Eyre Formation.|Sandstone, siltstone, mudstone; minor conglomerate, coal; predominantly alluvial deposits.|
20268|Winton Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
20268|Winton Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Mackunda Formation.||||||08-MAR-12
20268|Winton Formation|65489|5|Briefly described|p49, p53, p55, p57-61, p96, p155-156|Late Cretaceous|Late Cretaceous|Eromanga Basin. 1200m thick. Rapid non-marine deposition: c.1100m in c.8 m.y.||||Overlies Mackunda and Oodnadatta Formations. Is locally overlain unconformably by Mount Howie Sandstone.||
20268|Winton Formation|65925|5|Briefly described|p15, Appendix 2.|||Thousand-metre thick package deposited in low-energy fluvial to lacustrine environment.|||||Sandstone, shale, siltstone; coal seams.|
20268|Winton Formation|66131|6|Mentioned|p239|Cenomanian|Cenomanian|||||||
20268|Winton Formation|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin.||Unit in Rolling Downs Group.||Overlies Mackunda and Normanton Formations.|~1000m thick package of non-marine sandstones, shales and siltstones.|
20268|Winton Formation|66623|3|Fully described|p242, p245, pp256-257, pp266-267.|Cenomanian|Albian|Marks the stratigraphic top of the Rolling Downs Group throughout the Eromanga Basin. Correlates with upper half of Yalpunga Beds. Very poor outcrop; extensive post-deposition erosion reduced thickness from 0 to 1100 m. Fossils include vertebrates, plants, wood and microfossils.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain unconformably by fluvial Paleogene sedimentary rocks of Lake Eyre Basin, and by Cordillo Silcrete capping.|Medium-grained, cross-bedded sandstone with rounded intraclasts of siltstone and mudstone; calcareous labile sandstone, siltstone, carbonaceous and pyritic shale with intraclast conglomerate and minor coal; fresh volcanic detritus in sandstones.|07-JUN-13
20268|Winton Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|67119|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Non-marine.|||||Shale, siltstone, sandstone; minor coal horizons.|
20268|Winton Formation|67323|5|Briefly described|p86-87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Fluvial deposits. Underwent deep chemical weathering during Late Cretaceous to Palaeogene.||||Overlies Mackunda Formation.|Labile sandstone, siltstone, mudstone, minor coal.|
20268|Winton Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Cenomanian|Eromanga Basin. Maximum thickness of 1000m. Deposited in fluvial and lacustrine environments. Estimated porosity of 10-25% with likely favourable permeability for Carbon dioxide storage. See also p106, p108, p109, p111 fig ERO8, p115 tbl ERO2.||||Overlies the Mackunda Formation.|Interbedded sandstone, sandy siltstone, siltstone, mudstone and coal with minor intraformational conglomerate.|
20268|Winton Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||
20268|Winton Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
20268|Winton Formation|67784|5|Briefly described|p25, p31|Cenomanian|Albian|Northern Eromanga Basin. Up to 400m thick. Non-marine deposits.||||Overlies Mackunda Formation||08-FEB-18
20268|Winton Formation|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Coreena Member.||
20268|Winton Formation|68004|6|Mentioned|p204.|||Hosts opal. Ferruginisation increases toward the basal one-third of the profile.||||||
20268|Winton Formation|68068|5|Briefly described|Map legend|Cenomanian|Cenomanian|Eromanga Basin. Subsurface only. Fluvial to paludal-lacustrine. Fossil wood and leaves, freshwater bivalves, fish and vertebrates.||Unit in Neales River Group.||Conformably and gradationally overlies Mackunda Formation.|Dark grey-brown sandy silt-clay, finely laminated and cross-bedded, weakly bioturbated; basal portions carbonaceous to lignitic: lowest coal often taken as base of unit.|
20268|Winton Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Winton Formation as one unit.|||||Mudstone and siltstone.|
20268|Winton Formation|68206|6|Mentioned|p28|Cenomanian|Cenomanian|Great Artesian Basin. Marks a return to non-marine conditions after Barremian-Albian inundation.||||||
20268|Winton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Mackunda Formation.||
20268|Winton Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
20268|Winton Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Albian|Eromanga Basin.||||||
20268|Winton Formation|68731|6|Mentioned|pp209-211|||||||||
20268|Winton Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Fluvial to lacustrine. Late Albian maximum age. Opal is typically found in the upper 1-2 m of a claystone layer underlying a sandstone layer.||Of the Rolling Downs Group.|||Volcaniclastic.|18-JAN-22
20268|Winton Formation|68821|4|Described|p292 Fig.1, pp294-302, p307, p308 Fig.10|Cenomanian|Albian|Late Albian Maximum age. Contains ubiquitous disseminated pyrite. Preserved thickness is approximately 1200 m in the centre of the Eyre Basin. Fluvial to fluvial-lacustrine depositional environment.|97 - 93 Ma|Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises fluvial sandstone and siltstone.|
20268|Winton Formation|68901|5|Briefly described|p7 Fig. ii|||Eromanga Basin.||Rolling Downs Group|||Sandstone, siltstone, mudstone, calcareous in part.|27-SEP-18
20268|Winton Formation|69001|6|Mentioned|p18|Late Cretaceous||||||||
20268|Winton Formation|69019|4|Described|p83 Fig.20,p85,p94 Fig.24,p100-103,p169|Turonian|Cenomanian|Of Whitehouse (1953); formerly Winton Series (Dunstan, 1916). Named after Winton, Qld. Terrestrial deposition. Thickness from 0-150 m. Contains fossils of plants, lungfish teeth and possible dinosaur bone fragments. Of interest to explorers for biogenic coal seam gas.||Unit in Neales River Group.||Overlies Mackunda Formation. Is overlain disconformably by Eyre Formation and locally by Mount Howie Sandstone.|Dark khaki-grey to dark grey-brown, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained calcareous sandstone, sometimes feldspathic; seams of coal or lignite at/near the base; abundant plant fossils.|
20268|Winton Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93, p100|Turonian|Cenomanian|See also p105-106, p110, p112, p163, p191-192. Whitehouse (1955); formerly the Winton Series of Dunstan (1916) for freshwater sediments with coal seams in bores around Winton, Qld. Eromanga Basin. Resembles underlying Mackunda Formation. <40m thick. Contains plant, invertebrate and vertebrate fossils. Stratigraphic wells intersection data.||||Conformably overlies Mackunda Formation and Marree Subgroup. Is overlain disconformably by Eyre Formation.|Dark khaki-grey to grey, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained, calcareous sandstone and coal seams. Typically weathers to yellow or white kaolinitic sandstone.|
20268|Winton Formation|69454|5|Briefly described|p38:3, 13|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposition of this thick unit initiated hydrocarbon generation in underlying Permian and post-Permian source rocks.||||||12-JUL-16
20268|Winton Formation|69457|3|Fully described|p41:2-6, 9, 11-13, 17|Late Cretaceous|Early Cretaceous|Whitehouse (1955). Uppermost unit in the Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Fluviatile to paludal to lacustrine deposits; paralic, estuarine, deltaic and fluviatile near base. Maximum 620m thick in NT; c.1200m in the Patchawarra Trough in SA. Poorly exposed as highly weathered outcrops around dry lakes. Contains abundant micro- and macroflora and macrofauna. Late Albian to early Cenomanian. The seams of brown to black coal are uneconomic. Sediment loading by this thick unit is believed to have triggered hydrocarbon generation.||Manuka Subgroup.||Conformably overlies Mackunda Formation.|Claystone, siltstone and mudstone with interbedded very fine- to medium-bedded sandstone, and minor coal seams usually interbedded with carbonaceous mudstone; local minor intraformational conglomerate. Contains plant fragments and fossil wood.|12-JUL-16
20268|Winton Formation|69555|5|Briefly described|p43-44, p46-48|Turonian|Albian|Comprises the youngest Cretaceous strata of the Eromanga Basin. Fossil flora (palynological and macro) listed and described.||Rolling Downs Group|||Fossiliferous fine- to medium-grained, feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones, with very minor coal seams.|13-FEB-18
20268|Winton Formation|69582|6|Mentioned|p65|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|69594|5|Briefly described|p519, p526, p530-532, p563, p574|Cenomanian|Albian|Whitehouse (1955); Gray et al. (2002). Youngest deposits in the Eromanga Basin. Up to 1000m thick. The Mackunda-Winton boundary is difficult to pick. Unweathered outcrop is mainly well-cemented nodular sandstone; weathered outcrop is kaolinitised and ferruginised sandstones, mudstones and siltstone. Paralic, estuarine, deltaic and fluvial deposits in lower part; fluvio-lacustrine higher up. Contains a rich and diverse fossil flora, fauna and ichnofauna (listed and photographs); supports an economically important tourism industry. Detrital zircon plot.|~95 Ma (detrital zircon MDA: Greentree 2011).|||Conformably overlies Mackunda Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Much of the detritus is volcanogenic.|
20268|Winton Formation|69599|5|Briefly described|p599-600|Cretaceous|Cretaceous|||||Is overlain unconformably by Old Cork beds, Moses Sandstone, Edkins and Glendower Formations.||
20268|Winton Formation|69673|4|Described|p155 fig 127|Cretaceous|Cretaceous|Up to 620m thick.||Manuka Subgroup||Overlies Mackunda Formation, overlain by Mount Howie Sandstone Member|Claystone, siltstone and mudstone with interbedded very fine to fine to occasionally medium grained sandstone and minor coal seams.|
20268|Winton Formation|69742|5|Briefly described|p787, 788, 790, 793|Cenomanian|Albian|Great Artesian Basin. Hosts opal. Fluvial volcaniclastics. Geochemistry discussed.|||||Red-brown ironstone dominated by goethite and kaolinite with minor quartz and illite.|
20268|Winton Formation|69751|6|Mentioned|p35-38, 41|Cretaceous|Cretaceous|Eromanga Basin. Freshwater, broad fluvial-lacustrine environment of deposition (at least the upper part). Contains rich fossil assemblages; also silicified wood. Cenomanian-Turonian climate was seasonal and variable, with potential flooding and/or drought.|||||Fine- to medium-grained feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones; very minor coal seams.|
20268|Winton Formation|69797|5|Briefly described|p17 Fig.2|Late Cretaceous|Late Cretaceous|Geol. Prov: Eromanga Basin.||||||
20268|Winton Formation|69946|2|Defined|p27-28, p56-57, p124-125, p129|Late Cretaceous|Late Cretaceous|Eromanga Basin. Originally Winton Series (Dunstan, 1916), without formal definition. Renamed Winton Formation by Whitehouse (1955). His type section is 'blue shales and sandstones with intercalated coal seams met within the bores in and around Winton'. Distinguishing from Mackunda Formation is difficult in SA due to lack of coals, but easier in Qld due to coal seams, intraformational conglomerates and absence of marine fossils. 400-1100m thick. Late Albian - Cenomanian. Freshwater fossils listed. The top has been deeply (>40m) weathered.||||Conformably overlies Mackunda Formation. Is overlain unconformably by Eyre Formation.|Interbedded fine- to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates. Sandstone beds contain abundant fresh volcanogenic debris, lithics and feldspar.|
20268|Winton Formation|69947|5|Briefly described|p3, p9, p13 Fig.7.2|Late Cretaceous|Late Cretaceous|The final deposits in the Eromanga Basin. Is overlain by Tertiary sediments of the Lake Eyre Basin. On p9 the authors state: "the fluviolacustrine Winton Formation of the upper Marree Subgroup", which contradicts what appears in Fig.7.2.||||||
20268|Winton Formation|69948|6|Mentioned|p6; Figs.4.1, 18|||Eromanga Basin. Surface exposures of this and older units define the Birdsville Track Ridge.||||Overlies Mackunda Formation.||
20268|Winton Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Sandstone, siltstone, mudstone; calcareous in part.|
20268|Winton Formation|70383|5|Briefly described|p45|Cretaceous|Cretaceous|Eromanga Basin. Non-marine deposits.||||||
20268|Winton Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Non-marine mudstone and siltstone with subordinate interbedded coarse lithic and feldspathic labile sandstone.|18-JAN-22
20268|Winton Formation|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Coreena Member. Is overlain by Glendower Formation.||
20268|Winton Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
20268|Winton Formation|70821|4|Described|p21-24, p30-31, p33, p79-80, p82|Late Cretaceous|Late Cretaceous|See also p85-87, p115-116. Youngest Formation in the Eromanga Basin. Much of this unit in the southern Thomson region has been removed by erosion. Crops out as low breakaways, intensely weathered (kaolinitised and ferruginised): the weathering profile can be up to 95m deep. One of the two main groundwater resources in the Great Artesian Basin. Paralic, estuarine, deltaic and fluvial deposits in the lower part; fluvio-lacustrine in the upper. Fossil biota is dominated by fish, crocodiles, dinosaurs and pterosaurs. Late Albian to Cenomanian. Hydrochemistry mentioned; hydrostratigraphic properties.||Rolling Downs Group.||Overlies Mackunda Formation and locally the Wallumbilla Formation (conformably). Is overlain unconformably by Glendower Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Also pyritic black shale. Much of the clastic material is volcanogenic, presumably from volcanic arcs to the E.|
20268|Winton Formation|70823|5|Briefly described|p25-p27, p41, p43-p45, p78|Cenomanian|Cenomanian|Eromanga Basin. Up to 1200m thick. Deposited in a non-marine to marginal marine environment. Hosts lignite source rock. Age range derived from Bryan et al., 2012 and Tucker et al., 2013.|c. 99-93 Ma|||Overlies the Mackunda and Oodnadatta Formations. Overlain by the Mount Howe Sandstone.||
20268|Winton Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts lignite.||||Overlies the Mackunda Formation.||
20268|Winton Formation|70836|6|Mentioned|p474, 482|Turonian|Albian|Eromanga Basin. Preserves a rich and diverse vertebrate fauna including the only named Australian megaraptoran, Australovenator.|c.103-92 Ma (Tucker et al., 2013).|||||
20268|Winton Formation|70938|5|Briefly described|p816|Late Cretaceous|Late Cretaceous|Extensive, fluvial deposits. Paleocurrents and detrital zircons indicate a NE Queensland source.|||||Contains extensive labile volcanic detritus.|
20268|Winton Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29, p49|||Senior (1971). Eromanga Basin. 47m total thickness in Eulo 1 borehole. Non-marine deposits. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||||Overlies Coreena Member (Wallumbilla Formation).|Dark grey siltstone, weathering to white, finely-bedded mudstone and claystone mottled by goethite and hematite, with gypsum prevalent throughout the top of the unit; capped by a 5m-thick duricrust of porcellanite (white silicified mudstone).|
20268|Winton Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; fluvio-lacustrine siltstone and sandstones and locally coal-bearing.||||Overlain by Mount Howie Formation. Underlain by Mackunda Formation.|Fluvio-lacustrine siltstone and sandstones and locally coal-bearing.|
20268|Winton Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3 p4, Ch4 p6|Cenomanian|Albian|Eromanga Basin. Originally termed the Winton Series by Dunstan (1916) without formal definition. The name was changed to Winton Formation and a type section was designated in Queensland by Whitehouse (1955). The type section is described as "blue shales and sandstones with intercalated coal seams met within the bores in and around Winton". Hosts a major confined aquifer. Lithology, sedimentology, distribution and outcrop characteristics are discussed. This unit is generally thicker than 400m in the Cooper region and has a maximum thickness of 1100m in the northern Patchawarra Trough. Age derived on the basis of palynology and macrofossil assemblage. Spore-pollen zone is given in Ch5 p57. See also Ch4 p8, Ch4 p25, Ch5 p27-p28, Ch5 p30, Ch5 p33, Ch5 p56-p57, Ch5 p126-p127, Ch5 p130, Ch6 p9-p10, Ch7 p3, Ch7 p9, Ch7 p13, Ch9 p4-p5, Ch9 p10-p11, Ch9 p18, Ch10 p3.||||Conformably overlies the Mackunda Formation. Overlies the Oodnadatta Formation. Unconformably overlain by the Eyre Formation.|Interbedded fine to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates.|
20268|Winton Formation|71601|6|Mentioned|p120, p121|Turonian|Albian|Central west Qld. Ankylosaurian remains have been identified.||||||
20268|Winton Formation|71855|6|Mentioned|p20, p27, p30|||||||||
20268|Winton Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone and the Mackunda Formation.||
20268|Winton Formation|71864|4|Described|p8, p10, p13-p14, p16-p20, p26|||Intersected in GSQ Eulo 2 borehole between 2-23m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as non-marine fine sandstone and siltstone. Gamma log characteristics and magnetic susceptibility is provided.||||Overlies the Wallumbilla Formation.|Mottled, deeply weathered mudstone regolith with gypsum flakes throughout, blue siltstone and thin quartzose and lithic gravel bands.|
20268|Winton Formation|72297|5|Briefly described|p700, p724, p751, p758|Cretaceous|Cretaceous|Eromanga Basin. All coal seams are of uneconomic thickness and of poor quality. CSG exploration results not encouraging. Has a large kaolin deposit 35km W of Winton (70-80% kaolinite). Hosts QLD's opal fields within a 300km wide, NNW-trending belt from Hungerford to Kyuna.|||||White mudstone. Contains seams of subhydrous lignite - sub-bituminous black coal.|
20268|Winton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin. Confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Rumbalara Shale, Mackunda FZ.||
20268|Winton Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Shale, siltstone, sandstone that is non-marine with minor coal horizons.|
20268|Winton Formation|72915|6|Mentioned|p16|||Absent in the area of the Congararra 1 borehole (after Hawke and Cramsie, 1984).||||||
20268|Winton Formation|73106|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Shale, siltstone, sandstone. Non-marine, minor coal horizons.|
20268|Winton Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|73251|6|Mentioned|p62|Late Cretaceous|Late Cretaceous|Eromanga Basin. Non-marine to marginal marine.||||Underlain by Mackunda Formation and Oodnadatta Formation.||
20268|Winton Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
20268|Winton Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Oodnadatta Formation. Equivalent to Mackunda Formation.||
20268|Winton Formation|73393|6|Mentioned|p20||||||||Includes volcaniclastic sedimentary deposits.|
20268|Winton Formation|73479|5|Briefly described|p155, p156 Fig.2, p159-160|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97-93 Ma|||Overlies Oodnadatta Formation, unconformably underlies Eyre Formation||
20288|Wire Creek Sandstone|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
20288|Wire Creek Sandstone|22673|6|Mentioned|64|||Geological  province: Mount Isa Basin.||||||19-DEC-06
20288|Wire Creek Sandstone|23065|6|Mentioned|11|Proterozoic|Proterozoic|Geological  province: Lawn Hill Subprovince. Overlain by Peters Creek Volcanics.||||||19-DEC-06
20288|Wire Creek Sandstone|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20288|Wire Creek Sandstone|23395|5|Briefly described|p389|||||||||
20288|Wire Creek Sandstone|23396|5|Briefly described|p407 Fig.2|||||||||
20288|Wire Creek Sandstone|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Lawn Hill Subprovince (north).||||||07-NOV-08
20288|Wire Creek Sandstone|31421|6|Mentioned|p509|||||||||
20288|Wire Creek Sandstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|36012|3|Fully described|Table 3|||See also p11, 16.||||||19-DEC-06
20288|Wire Creek Sandstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|37568|6|Mentioned|Fig.5|||||||||
20288|Wire Creek Sandstone|38237|6|Mentioned|Fig.3|||||||||
20288|Wire Creek Sandstone|38584|4|Described|p15|||||||||
20288|Wire Creek Sandstone|39445|5|Briefly described|Table 2|||See also p39.||||||19-DEC-06
20288|Wire Creek Sandstone|39497|6|Mentioned|p7|||See also Fig.4||||||
20288|Wire Creek Sandstone|39685|6|Mentioned|p407|||||||||
20288|Wire Creek Sandstone|39925|6|Mentioned|p334|||||||||
20288|Wire Creek Sandstone|40840|6|Mentioned|Map legend|||||||||
20288|Wire Creek Sandstone|41319|6|Mentioned|Fig.1|||||||||
20288|Wire Creek Sandstone|41721|4|Described|p27|||Conformably overlain by Peters Creek Volcanics.Thickness: <70m. Medium to coarse sandstone with scattered pebbles, mostly quartz and volcanics; lenticular conglomeratic beds + clasts up to 30cm are common. Part of the Lawn Hill Platform sequence.||||||02-AUG-07
20288|Wire Creek Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
20288|Wire Creek Sandstone|42812|6|Mentioned|p10|||||||||
20288|Wire Creek Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic" age.||||||19-DEC-06
20288|Wire Creek Sandstone|45166|6|Mentioned|p14|||||||||
20288|Wire Creek Sandstone|46804|6|Mentioned|p154|||||||||
20288|Wire Creek Sandstone|49001|2|Defined|p5|Carpentarian|Carpentarian|||||||
20288|Wire Creek Sandstone|63113|6|Mentioned|p1214 Fig.2.|||Southern Murphy Inlier, Lawn Hill platform, Leichhardt Superbasin. Written as Wire Cr Sst||||Correlated with Bottle Tree Formation and Mount Guide Quartzite. Is overlain by Buddawadda Basalt.||
20288|Wire Creek Sandstone|63866|5|Briefly described|p56|||Crops out on the southern flank of the Murphy Inlier.||||Equivalent to the Guide Supersequence.||
20288|Wire Creek Sandstone|64724|5|Briefly described|p46|Statherian|Statherian|Unit of the Leichhardt Superbasin (South Nicholson Basin), deposited during the Leichhardt Extension (1800-1750 Ma)||||||
20288|Wire Creek Sandstone|65228|6|Mentioned|Fig.07.|||Southern McArthur Basin.||||Is overlain by Peters Creek Volcanics.||
20288|Wire Creek Sandstone|67323|4|Described|GIS attrib tbl, Solid Geology Map, p9|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Lawn Hill Platform, Leichhardt Superbasin. Camooweal-Murphy Domain, Mount Isa Inlier.|1847 +/- 13 Ma (maximum depositional age).|Tawallah Group.||Correlated with Westmoreland Conglomerate and Mount Guide Quartzite.|Coarse gritty sandstone with scattered quartz pebbles; cobble and boulder conglomerate lenses|
20288|Wire Creek Sandstone|69383|4|Described|p49-52|Paleoproterozoic|Paleoproterozoic|McArthur Basin, base Lawn Hill Platform. Up to 70 m thick. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1847+/-13 Ma|||Unconformable on Murphy Inlier basement. Stratigraphic equivalent to Westmoreland Conglomerate.|Medium- to coarse-grained cross-bedded sandstone with scattered pebbles mostly of quartz and volcanics, deposited in braided river and alluvial fan environments.|
20288|Wire Creek Sandstone|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||||12-JUL-16
20288|Wire Creek Sandstone|69433|4|Described|p18:1-4|Statherian|Orosirian|Sweet (1981). Northern succession, Lawn Hill Platform. Unconformably overlies igneous and metamorphic rocks of the Murphy Inlier. Up to 70m thick. Fluvial braided river and alluvial fan deposits. Detrital zircon age. Correlated with Westmoreland Conglomerate of the Tawallah Group (McArthur Basin), and possibly with Don Creek Sandstone.|<1847 +/- 13 Ma (maximum deposition age).|||Unconformably overlies the Nicholson Granite Complex and Cliffdale Volcanics. Is overlain, probably conformably, by Peters Creek Volcanics.|Commonly cross-bedded, medium to coarse sandstone with scattered pebbles, mostly of vein quartz and volcanic rocks. Lenticular conglomerate beds with clasts to 30cm are common. Basal conglomerate bed is often developed.|12-JUL-16
20288|Wire Creek Sandstone|69591|5|Briefly described|p33-34, p58|||Camooweal-Murphy Domain, Leichhardt Superbasin. Fluvial deposits.|1847 +/- 13 Ma (MDA: Carson et al., 2011).|||Correlated with Westmoreland Conglomerate.|Coarse gritty sandstone with scattered quartz pebbles; cobble and boulder conglomerate lenses.|
20288|Wire Creek Sandstone|69673|5|Briefly described|p51|||Considered to be equivalent to the Tawallah Group of the McArthur Basin. Up to 70m thick.||||Unconformably overlain by Fickling Group|Sandstone with scattered pebbles, mostly of vein quartz and volcanic rocks.|
20288|Wire Creek Sandstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Tawallah Group.||Unconformably overlies Murphy Metamorphics. Is overlain by Peters Creek Volcanics.|Sandstone with scattered quartz pebbles, medium- to coarse-grained, cobble and boulder conglomerate lenses.|
20288|Wire Creek Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1847+/-13 Ma (MDA: U-Pb zircon LA-ICPMS).||||Cross-bedded sandstone.|
20288|Wire Creek Sandstone|71606|5|Briefly described|p137|Statherian|Statherian|South Nicholson Basin.||||Overlain by Peters Creek Volcanics. Underlain unconformably by Murphy Metamorphics.||
20288|Wire Creek Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform. Grouped with lower part of Peters Creek Volcanics on this map.||Lower Peters Creek Volcanics.||||05-MAR-20
20288|Wire Creek Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the west of the South Nicholson Basin.||||Shown as unconformably overlying Nicholson Granite Complex and underlies Peters Creek Volcanics.||
20288|Wire Creek Sandstone|72527|4|Described|p7, p9, p176-180, p193, p194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Previous dating gave 1847+/-13 Ma from site 20 km further east. Depositional age bracketed  by underling and overlying units to 1845-1725 Ma range. Type locality in Hedleys Creek 1:100k area, Qld. Maximum thickness 70 m in Qld. Sample is of feldspathic coarse sandstone. Braided stream and/or alluvial fan depositional environment. Ages derived for this unit are similar to Westmoreland Conglomerate.|1854+/-4 Ma max.dep.age, Pb/Pb SHRIMP.|Tawallah Group||Equivalent to Westmoreland Conglomerate. Unconformably underlies Carrara Range Group and Peters Creek Volcanics and unconformably overlies Murphy Metamorphics and Nicholson Granite.|Coarse-grained, gritty quartz sandstone, occasionally cross-bedded, with pebble lags and local cobble to boulder conglomerate lenses, containing rounded clasts of predominantly white vein quartz, quartzite, felsic volcanics and rarely, granite.|
20288|Wire Creek Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the west part of the South Nicholson Basin||||Unconformably overlies Nicholson Granite Complex and underlies Peters Creek Volcanics.||
20288|Wire Creek Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region. Age range indicated to be quite uncertain, with ? above and below.||||||
20296|Wirralie Granodiorite|23052|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
20296|Wirralie Granodiorite|23161|4|Described|p42 table5|Early Permian|Late Carboniferous|||||||
20296|Wirralie Granodiorite|42701|2|Defined|p94|Early Permian|Late Carboniferous|Age not known. Assigned on lithological similarity. Reserved as Wirrilie Granodiorite [resn misspelt||||||
20296|Wirralie Granodiorite|44245|5|Briefly described|Map Legend|Permian|Carboniferous|||||||
20296|Wirralie Granodiorite|60659|5|Briefly described|p17|||Includes biotite-hornblende granodiorite, hornblende-rich granodiorite, porphyritic granodiorite and microgranite. Intrudes the Bulgonunna Volcanic Group.||||||07-FEB-11
20296|Wirralie Granodiorite|69593|5|Briefly described|p495|Permian|Late Carboniferous|Burdekin Falls Subprovince.|~297-290 Ma.||||I-type. Mainly biotite granite and microgranite, intrusive rhyolite, and biotite to (pyroxene-)hornblende-biotite granodiorite.|
20296|Wirralie Granodiorite|70740|5|Briefly described|p34, p130|||Outcrop and geophysical characteristics briefly discussed.||||Overlain by the Suttor Formation. Intrudes the Anakie Metamorphic Group.|Biotite-hornblende granodiorite, tonalite and altered granite.|
20296|Wirralie Granodiorite|73035|5|Briefly described|Map legend|Permian|Permian||||||Biotite hornblende granodiorite, altered granite.|
20310|Wiseman Formation|24615|5|Briefly described|CD|Late Permian|Late Permian|[Pwyw].  Calcareous sandstone, mudstone and siltstone.||||||
20310|Wiseman Formation|30141|5|Briefly described|p134|||||||||
20310|Wiseman Formation|30451|6|Mentioned|Fig.8|||See also P60. Refers Derrington & Morgan (1960)||||||
20310|Wiseman Formation|33363|6|Mentioned|p116|||U.Perm.||||||
20310|Wiseman Formation|35426|6|Mentioned|p659|||||||||
20310|Wiseman Formation|36739|6|Mentioned|Fig.4|||||||||
20310|Wiseman Formation|41666|6|Mentioned|Fig.1|||||||||
20310|Wiseman Formation|44381|14|Not recorded|p6|||Equivalent of Gyranda Formation.||||||
20310|Wiseman Formation|44514|2|Defined|p27,33||Late Permian|Conformably overlies Banana Formation. Fossil wood.||||||15-JUL-13
20310|Wiseman Formation|44571|2|Defined|p206-207,Fig.28|||||||||
20310|Wiseman Formation|50215|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Gyranda Subgroup. Calcareous lithic sandstone. mudstone and siltstone, rare coal.||||||18-JUN-09
20310|Wiseman Formation|50273|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Gyranda Subgroup (Blackwater Group). Calcareous lithic sandstone, mudstone, siltstone and rare coal.||||||
20310|Wiseman Formation|64856|3|Fully described|p42, p56-58, p60, p62 Fig.12, p66|Late Permian|Late Permian|Derrington et al. (1959) after Glover (1954, 1955). Bowen Basin. Medium to coarse grained sandstones, interbedded with mudstones and siltstones conformably overlies Banana Formation. Overlain by Baralaba Coal Measures. Correlated with Burunga Formation and in part with Gyranda Formation. Age from palynoflora (unit APP5). Thickness 321m.|| ||||29-NOV-17
20310|Wiseman Formation|64857|5|Briefly described|p121-124, p113 Fig.3|Late Permian|Late Permian|Overlies Banana Formation.||||||
20310|Wiseman Formation|64858|6|Mentioned|p181 Tb. 1, p180 Fig.2|Late Permian|Late Permian|Bowen Basin.||||||30-NOV-09
20310|Wiseman Formation|64859|6|Mentioned|p196, 225|Permian|Permian|Oil and gas source rocks.||||||
20310|Wiseman Formation|65388|5|Briefly described|p195-196, p161 Fig. 62, 163, 193, 194|Late Permian|Late Permian|Of Gyranda Subgroup, Blackwater Group. Conformably overlies Banana Formation. Conformably overlain by Baralaba Coal Measures. Recognised in stratigraphic holes and petroleum wells. Consists of siltstone, sandstone and lesser silty mudstone. The upper part of the Gyranda Subgroup intersected in GSQ Mundubbera 5 from 214-521m is  a reference section (Gray and Heywood, 1978).||||||
20310|Wiseman Formation|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
20310|Wiseman Formation|68679|5|Briefly described|p377, p381-382|Permian|Permian|Derrington et al. (1959). E Taroom Trough, Bowen Basin. 321m thick. Progradational delta, prodelta deposits.||||Overlies Banana Formation. Is overlain by Baralaba Coal Measures.|Mudstone, siltstone, medium- to coarse-grained lithic sandstone, tuff, minor coal. Coarsening-upwards successions.|
20316|Withersfield Quartz Syenite|42747|5|Briefly described|Fig.9 P38|||see also Table 1. Reserved as Withersfield Granite.||||||
20316|Withersfield Quartz Syenite|43029|2|Defined|p24||Late Carboniferous|K-Ar dating of 287-306 Ma. See also Fig.2,p16.||||||
20316|Withersfield Quartz Syenite|43204|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||23-DEC-11
20316|Withersfield Quartz Syenite|43213|3|Fully described|p17, p95-97, p114-115, p117, p121-124|Carboniferous|Carboniferous|See also p163, p174-175, p179, p209-210, p226, p234, p241-242. Intrudes rocks of the Drummond Basin. Outcrop, geophysical properties and type locality described. Geochemistry, modal and chemical analyses and geophysics detailed. Biotite and hornblende K-Ar ages. This unit may be age-equivalent to the Bulgonunna Volcanic Group which overlies the N Drummond Basin. Contains olivine gabbro and dolerite which may represent feeders for (Hoy Basalt) flows.|287 Ma and 306 Ma (Webb and McDougall, 1969).|||Intrudes Telemon and Mount Hall Formations and Raymond Sandstone. Is intruded by Hoy Basalt.|Pink, fine- to medium-grained, equigranular hornblende-biotite quartz syenite to quartz monzonite.|
20316|Withersfield Quartz Syenite|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Drummond Basin. Connors Subprovince.||||Intrudes Connors Volcanic Group.||25-NOV-13
20316|Withersfield Quartz Syenite|68731|5|Briefly described|p133, p134 Fig 3F3.1|Carboniferous|Carboniferous|Comprises a 4 km wide x 6 km long pluton that occurs 10 km west of Sapphire.||||||
20316|Withersfield Quartz Syenite|68900|6|Mentioned|p4|Carboniferous|Carboniferous|Drummond Basin.||||||
20316|Withersfield Quartz Syenite|69599|5|Briefly described|p644|Carboniferous|Carboniferous|Headwaters of Spring Creek, W of Rubyvale.||||Is overlain by Hoy Basalt.||
20316|Withersfield Quartz Syenite|69952|6|Mentioned|p131|||Intrudes Early Carboniferous Drummond Basin rocks to the W of Anakie. Undated, but could be Late Carboniferous, the age of an unnamed diorite dated at c.313 Ma (Cross et al., 2015).||||||
20337|Witty Gravel|39445|5|Briefly described|Table 14|||||||||
20337|Witty Gravel|44687|2|Defined|p227|Cenozoic|Cenozoic|Semi-consolidated gravel, clay and sandstone. 30 ft thick.||||Disconformable over Sugars Basalt, Mount Crosby Formation, Colleges Conglomerate, Tivoli-Cooneana Formations undiff.||21-MAR-13
20337|Witty Gravel|44703|14|Not recorded|Map||Cenozoic|||||||19-NOV-08
20337|Witty Gravel|44705|14|Not recorded|p1,2|||||||||
20337|Witty Gravel|44708|14|Not recorded|p3,21,Sheet2,section||Cenozoic|||||||19-NOV-08
20337|Witty Gravel|69599|5|Briefly described|p586|Pliocene|Pliocene|||||Correlated with Lone Pine Gravel.||
20351|Wolfang Coal Measures|23008|5|Briefly described|p461 Fig.3|Permian|Permian|||||||
20351|Wolfang Coal Measures|36172|6|Mentioned|Appendix|||||||||
20358|Wollogorang Formation|22432|4|Described|p20-22, Fig.22|Statherian|Statherian|U-Pb SHRIMP ages 1730 +/- 3Ma , 1723 +/-4Ma.||||||19-DEC-06
20358|Wollogorang Formation|22457|5|Briefly described|P31|Statherian||Age of lower unit is 1730 Ma.||||||19-DEC-06
20358|Wollogorang Formation|22538|6|Mentioned|App1 P722|||||||||
20358|Wollogorang Formation|22644|5|Briefly described|5 fig 2|||Geological  province: McArthur Basin. ?Of the Murphy Metamorphics. Overlain by Gold Creek Volcanics.||||||19-DEC-06
20358|Wollogorang Formation|22670|6|Mentioned|52, fig 1,53,55|||Geological province: McArthur Basin. Of the Tawallah Group. Formation written as 'Fmt' in text||||||19-DEC-06
20358|Wollogorang Formation|22853|3|Fully described|13|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness 150 m. Underlain by Settlement Creek Volcanics||||||19-DEC-06
20358|Wollogorang Formation|23065|5|Briefly described|16|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1730+/-3Ma.||||||19-DEC-06
20358|Wollogorang Formation|23395|5|Briefly described|p389|||||||||
20358|Wollogorang Formation|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the Tawallah Group. Age: 1723+/-4Ma.||||||19-DEC-06
20358|Wollogorang Formation|23397|5|Briefly described|p480|Statherian|Statherian|||||||
20358|Wollogorang Formation|23398|4|Described|p435|Statherian|Statherian|||||||
20358|Wollogorang Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
20358|Wollogorang Formation|23776|5|Briefly described|p705 Fig 2|||Of Tawallah Group.||||||
20358|Wollogorang Formation|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with McCaw Formation (Katherine River Group).  Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|23963|5|Briefly described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group. Max. Thickness: 100m. Overlies the Settlement Creek Volcanics||||||
20358|Wollogorang Formation|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
20358|Wollogorang Formation|24048|5|Briefly described|p36|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|24179|4|Described|p82, 83, 84 Fig. 2|||Of the Tawallah Group.  Overlies the Settlement Creek Volcanics.  Overlain by the Gold Creek Volcanics.  Max. Thickness: 150m.  Geological Province:  McArthur Basin.  Age: 1729 +/- 4 and 1730 +/- 3 Ma (U-Pb).||||||19-DEC-06
20358|Wollogorang Formation|24432|5|Briefly described|p565 Fig.2|Statherian|Statherian|Of Upper Tawallah Group. Carbonate. Geological Province: Southern McArthur Basin.||||||
20358|Wollogorang Formation|26310|4|Described|p7, Fig. 2, Table 1|Proterozoic|Proterozoic|Dolomite, chert breccia, siltstone, sandstone. Maximum Thickness: 1000 feet.||||||
20358|Wollogorang Formation|32519|4|Described|Table 1|||||||||
20358|Wollogorang Formation|32660|5|Briefly described|Table 4|||||||||
20358|Wollogorang Formation|32904|6|Mentioned|p89|||||||||
20358|Wollogorang Formation|33214|6|Mentioned|Fig.1|||||||||
20358|Wollogorang Formation|33665|5|Briefly described|p368|||||||||
20358|Wollogorang Formation|35114|6|Mentioned|p203|||||||||
20358|Wollogorang Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20358|Wollogorang Formation|35776|4|Described|p819|||See also Fig.1 and Table 1.||||||
20358|Wollogorang Formation|36012|3|Fully described|Table 2|||See also p16.||||||19-DEC-06
20358|Wollogorang Formation|37568|5|Briefly described|p78|||See also p75.||||||19-DEC-06
20358|Wollogorang Formation|37569|6|Mentioned|p91|||||||||
20358|Wollogorang Formation|37670|6|Mentioned|p71|||||||||
20358|Wollogorang Formation|38582|6|Mentioned|Fig.3|||||||||
20358|Wollogorang Formation|39210|6|Mentioned|p50|||||||||
20358|Wollogorang Formation|39445|6|Mentioned|p39|||Now Fickling Group.||||||
20358|Wollogorang Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20358|Wollogorang Formation|40105|6|Mentioned|p317|||||||||
20358|Wollogorang Formation|40109|4|Described|p302|||||||||
20358|Wollogorang Formation|40259|6|Mentioned|Table 1|||||||||
20358|Wollogorang Formation|40691|6|Mentioned|p7|||||||||
20358|Wollogorang Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20358|Wollogorang Formation|41220|6|Mentioned|Fig.3|||||||||
20358|Wollogorang Formation|41721|3|Fully described|p23|||Of the Tawallah Group. Overlain by Gold Creek Volcanics; overlies Settlement Creek Volcanics. Thickness: 180m. Geological province: McArthur Basin. Dolomite, siltstone and sandstone.||||||01-AUG-07
20358|Wollogorang Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
20358|Wollogorang Formation|42385|4|Described|p13, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Dark grey weathering, thinly bedded dololutite with rare columnar stromatolites. Parts have been reassigned to Aquarium Fm. and Settlement Creek Volcanics. Max. thick: <150m.||||||18-SEP-07
20358|Wollogorang Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
20358|Wollogorang Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||Not shown in schematic sections.|Dololutite, rare columnar stromatolites; dololutite breccia or shale with evaporaite mineral casts; upper unit of ferruginous sandstone, quartarenite, dolomitic in places. Detailed lithology given.|09-NOV-11
20358|Wollogorang Formation|42639|4|Described|p14, Table 4 p11|||||||||
20358|Wollogorang Formation|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
20358|Wollogorang Formation|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Sandstone, mudstone, dololutite.||||||19-OCT-05
20358|Wollogorang Formation|42812|3|Fully described|p23, Table 3|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|42873|5|Briefly described|p109|||see also Fig.1, p110.||||||19-DEC-06
20358|Wollogorang Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterozoic" age.||||||19-DEC-06
20358|Wollogorang Formation|43036|3|Fully described|p29|||Of the Tawallah Group.||||||19-DEC-06
20358|Wollogorang Formation|44112|6|Mentioned|p43,49|||||||||
20358|Wollogorang Formation|44271|2|Defined|p39,41|||Overlies Peters Creek Volcanics.||||||
20358|Wollogorang Formation|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
20358|Wollogorang Formation|44274|14|Not recorded|p8|||||||||
20358|Wollogorang Formation|44275|14|Not recorded|Map Legend|||||||||
20358|Wollogorang Formation|44280|2|Defined|p5-6,Tb.1,map||Neoproterozoic|||||||
20358|Wollogorang Formation|44287|14|Not recorded|p.8,18, opp.7|||opp.8. (E53-3).||||||
20358|Wollogorang Formation|44288|14|Not recorded|map legend||Paleoproterozoic|||||||07-NOV-08
20358|Wollogorang Formation|44305|14|Not recorded|p.6,12,13|||(E53-8). opp.6,18.||||||
20358|Wollogorang Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44436|5|Briefly described|p.4,7-9,12,opp.7,map|||(E53-4).||||||02-DEC-04
20358|Wollogorang Formation|44437|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group.  Dolomitic siltstone and feldspathic sandstone, algal dolomite, dolarenite; silty and sandy dolomite; nodular dolomitic siltstone.  Conformably overlies Settlement Creek Formation; conformably overlain by Masterton Formation.||||||07-NOV-08
20358|Wollogorang Formation|44459|14|Not recorded|p.7,13, opp.p.6, map|||(E53-2).||||||
20358|Wollogorang Formation|44460|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44473|14|Not recorded|p.8, opp. p.7|||(E53-7).||||||
20358|Wollogorang Formation|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44530|14|Not recorded|p.4,9, opp.8|||(D53-15).||||||
20358|Wollogorang Formation|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
20358|Wollogorang Formation|44989|2|Defined|p.116-7, p.115-119|||Tb.II, IV. On many pages. Underlies Constance Sandstone [this is wrong]. (E54-5,E53-8).||||||22-FEB-18
20358|Wollogorang Formation|45162|2|Defined|p32|Proterozoic|Proterozoic|tyep section location given.||||||22-FEB-18
20358|Wollogorang Formation|45287|14|Not recorded|p.223,226|||||||||
20358|Wollogorang Formation|46804|6|Mentioned|p154|||||||||
20358|Wollogorang Formation|46915|6|Mentioned| P156|||||||||
20358|Wollogorang Formation|46968|6|Mentioned|Fig.2|||||||||
20358|Wollogorang Formation|47013|6|Mentioned|p333|||||||||
20358|Wollogorang Formation|60483|5|Briefly described|p7 Fig. 5, p29|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Age: 1730+/-3Ma, 1729+/-4Ma. Geological Province: McArthur Basin. Carbonaceous unit.||||||07-NOV-08
20358|Wollogorang Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Warramana Sandstone and Gold Creek Volcanics, underlain by Settlement Creek Volcanics.||||||
20358|Wollogorang Formation|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Overlies the Settlement Creek Dolerite. Overlain by the Gold Creek Volcanics. Mudstone, dolostone, shale, siltstone and variably-dolomitic sandstone.||||||07-NOV-08
20358|Wollogorang Formation|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Wollogorang Fm.|1730+/-3 Ma U-Pb SHRIMP (after Page et al. 2000)|||||
20358|Wollogorang Formation|63112|6|Mentioned|p1191 Fig.2,p1192,p1194-1198,p1200-1206|||Calvert Superbasin. Ages from volcaniclastic mudstones and tuffs. 100-270 m thick.|1734 +/- 5 Ma (lower) to 1722 +/- 4 Ma (upper).|Unit in Big Supersequence.||Is overlain by Gold Creek Volcanics.|Lower dolostone-mudstone-carbonaceous shale unit; upper coarse-grained sandstone-dominated unit grading into stromatolitic dolostone facies.|
20358|Wollogorang Formation|63866|5|Briefly described|p54|||Two additional depositional ages of 1729 +/- 4 and 1722 +/- 4 Ma are also provided from Page et al., 2000.|1735 +/- 6 Ma (Page et al., 2000)||||Basal shales and carbonate-rich sedimentary rocks that contain green 'tuff' horizons.|
20358|Wollogorang Formation|64726|6|Mentioned|p86 Table 1, p87.||||1730 +/- 3 Ma.|||||
20358|Wollogorang Formation|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
20358|Wollogorang Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2, p369 |Statherian|Statherian||1730 +/- 3 Ma; 1729 +/- 4 Ma; 1723 +/- 4 Ma.|Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
20358|Wollogorang Formation|65228|4|Described|p7, p22, p25, Figs.02, 04-07.|Statherian|Statherian|McArthur Basin. Diagnostic carbonate lithofacies of this unit  also occurs in the McCaw Formation, Katherine River Group [ i.e. they are considered time-equivalents?]. U-Pb SHRIMP ages from tuff beds (Page et al. 2000).|1730 +/- 3 Ma to 1723 +/- 4 Ma.|Unit in Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics and Warramana Sandstone.|Red mudstone, carbonate, black shale, sandstone.|13-DEC-17
20358|Wollogorang Formation|65232|5|Briefly described|p9|||Of Tawallah Group. Age: 1730-1720 Ma (tuff, OZCRHON). Correlated with upper part of Katherine River Group. Geol. Prov: McArthur Basin.||||||09-FEB-10
20358|Wollogorang Formation|65337|6|Mentioned|p18.|||Southern McArthur Basin. Contains 'beehive stromatolites'.||||||
20358|Wollogorang Formation|65340|3|Fully described|p5, p13 Tb4, pp16-27, p37, pp76-78, p92|||Was in sedimentological continuum with Aquarium Formation prior to intrusion by Settlement Creek Dolerite. Epeiric or marginal marine salina, intertidal, deep anoxic, storm- and wave-influenced shelf, shoreface depositional environments. MSc and related papers published (Jackson 1982, 1985). Hosts copper mineralisation in veins and disseminated in dolostone, at Foelsche River. Proposed as source of reduced hydrocarbon-bearing fluids into overlying Gold Creek Volcanics, causing deposition of siegenite and chalcopyrite.|c.1730 Ma (Jackson et al. 1997).|Unit in Tawallah Group.|Includes Wollogorang Formation - Lower and Wollogorang Formation - Upper.|Nonconformably overlies and is locally intruded by Settlement Creek Dolerite. Is intruded by Packsaddle Microgranite. Is overlain by Gold Creek Volcanics.|Lower red/brown mudstone, dolostone, carbonaceous shale, dolomitic siltstone; upper dolomitic sandstone, dolarenite and stromatolitic dolostone and chert; hornfelsed and brecciated adjacent to Settlement Creek Dolerite and Packsaddle Microgranite.|
20358|Wollogorang Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics.|Thinly-bedded dololutite, pyritic with ovoid nodules, rare columnar stromatolites; local basal dololutite breccia or shale with evaporite mineral casts; upper unit of ferruginous, cross-bedded sandstone and white quartz arenite, locally dolomitic.|
20358|Wollogorang Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p33|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Calvert Superbasin.|1729 +/- 4 Ma to 1722 +/- 4 Ma.|Tawallah Group.|||Siltstone, dolomite, lithic and dolomitic sandstone.|
20358|Wollogorang Formation|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 150 m thick.||Tawallah Group||Overlies (conformably) Wununmantyala Sandstone or Settlement Creek Volcanics. Overlain conformably by Gold Creek Volcanics; unconformably by Masterton Sandstone.|Dolostone; coarse-grained quartz sandstone; thinly bedded to laminated siltstone, shale; minor breccia, conglomerate; basal mudstone, siltstone.|
20358|Wollogorang Formation|69418|4|Described|p3:15|||Hydrocarbon-bearing fluids from this unit have been proposed as an agent in formation of copper deposits in breccia pipes in the Redbank field.||||Is overlain by Gold Creek Volcanics.||12-JUL-16
20358|Wollogorang Formation|69430|4|Described|p15:3, 9-12, 44-48, 62|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin. Over 350m thick. Lower part is shallow-marine; upper part is locally reworked fluvial deposits in shoreface and intertidal channels. There is a paraconformity between lower and upper parts. Hosts Cu-bearing breccia pipes (described in some detail). Fair to good conventional hydrocarbon reservoirs occur.|1730 +/- 3 Ma; 1723 +/- 4 Ma.|Tawallah Group.||Overlies, and is also intruded at higher levels by, Settlement Creek Dolerite. Is overlain conformably by Warramana Sandstone and Gold Creek Volcanics. Is intruded by Packsaddle Microgranite.|Mudstone, dolostone, carbonaceous shale, dolomitic siltstone, dolomitic sandstone, dolarenite and stromatolitic dolostone and chert, lithic sandstone, evaporitic carbonaceous shale.|12-JUL-16
20358|Wollogorang Formation|69545|5|Briefly described|p99, p103, p105|Paleoproterozoic|Paleoproterozoic|A significant quantity of aromatic hydrocarbons generated in this unit was transported into the overlying Barney Creek Formation by mineralising fluid.||||Is overlain by Barney Creek Formation.||
20358|Wollogorang Formation|69591|5|Briefly described|p38, p56|||Camooweal-Murphy Domain, Mount Isa Province. N of the Murphy Tectonic Ridge. Part of Tawallah Supersequence. Shallow subaqueous deposits. Similar to sedimentary units in the Peters Creek Volcanics.||Tawallah Group.|||Siltstone, dolomite.|
20358|Wollogorang Formation|69673|5|Briefly described|p16 fig 13, p24, p25, p32, p33, p40|||Mixed carbonates and clastic sedimentary rock. Roughly 160m thick. Peperitic contact with Gold Creek Volcanics. Subdivided into dolostone and sandstone units by paraconformity. Some source rock potential.|1730 +/- 3 Ma, 1723 +/- 4 Ma|Tawallah Group||Overlain by Warramana Sandstone, Echo Sandstone, conformably overlain by Gold Creek Volcanics, Overlies Settlement Creek Dolerite|Dolostone, mudstone and sandstone.|
20358|Wollogorang Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Settlement Creek Volcanics. Is overlain by Gold Creek Volcanics.|Two facies mapped separately. Dolomitic sandstone, dolomite, stromatolitic dolomite, oolitic dolomite; dolomitic and quartz sandstone, ferruginous in parts, feldspathic, dolomitic siltstone.|
20358|Wollogorang Formation|71374|6|Mentioned|p6|||McArthur Basin.||Tawallah Group||Unconformably overlain by the Masterton Sandstone.||
20358|Wollogorang Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1729+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Green ash tuff.|
20358|Wollogorang Formation|72377|5|Briefly described|iii|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Likely time-equivalent with Dhunganda Formation (c. 1730-1723 Ma).|c. 1730-1723 Ma|Unit of Tawallah Group.||||
20358|Wollogorang Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin. Three U-Pb zircon sedimentary depositional ages given 1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma.|1723+/-4 Ma|Tawallah Group||Overlies Settlement Creek Dolorite and underlies Gold Creek Volcanics and Warramana Sandstone.||
20358|Wollogorang Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin.|1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma.|Tawallah Group||Underlain by Settlement Creek Dolerite. Partly overlain by Warramana Sandstone and Gold Creek Volcanics.||
20358|Wollogorang Formation|72912|5|Briefly described|p5 Fig.3, p19, p31 Fig.11, p36.|Statherian|Statherian|Located in the Beetaloo Sub-basin and the Batten Fault Zone in the Southern McArthur Basin.  Hydrocarbon shows known. TOC is discussed in addition to organic richness. Three U-Pb zircon sedimentary depositional ages given 1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma. See also p37 Fig.14.|1723+/-4 Ma|Tawallah Group||Overlies Settlement Creek Dolorite and underlies Warramana Sandstone and Gold Creek Volcanics.||15-MAR-21
20358|Wollogorang Formation|73042|6|Mentioned|p4, p12|Statherian|Statherian|Southern McArthur Basin, Calvert Superbasin. Southern McArthur Basin, Roper Superbasin. Geochronology is U-Pb zircon sedimentary depositional ages (?maximum depositional age).|1730+/-3 Ma, 1729+/-4 Ma, 1723+/-4 Ma|Tawallah Group||Underlain by Settlement Creek Dolorite. Partly overlain by Gold Creek Volcanics and Warramana Sandstone.||
20358|Wollogorang Formation|73083|6|Mentioned|p39-40|||||||Overlain by Echo Sandstone.||
20358|Wollogorang Formation|73280|6|Mentioned|p1, p4-5, App.1A, App.1B, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
20358|Wollogorang Formation|73412|5|Briefly described|p2, 4, 8|||Southern McArthur Basin.|1730-1725 Ma (SHRIMP: Page et al., 2000).|Tawallah Group.||Overlies Settlement Creek Dolerite. Is overlain by Gold Creek Volcanics and Warramana Sandstone.||
20383|Wolverton Granite|23420|5|Briefly described|p 136||Permian|Also see Wolverton Adamellite. In the Kennedy Province||||||
20383|Wolverton Granite|42327|6|Mentioned|Fig.22 P15|||Variation on Wolverton Adamellite?||||||
20383|Wolverton Granite|49769|6|Mentioned|Fig.1,p2|||||||||
20383|Wolverton Granite|71792|5|Briefly described|p25, p33, p51|Early Permian|Early Permian|Age is derived from Cross et al (in prep) and is interpreted as the emplacement age.|280.4 +/- 1.5 Ma (SHRIMP U-Pb)|||Faulted against the Wigan Granite.|Leucocratic biotite monzogranite to syenogranite and aplite.|
20383|Wolverton Granite|71849|3|Fully described|p1, p4, p6, p8, p11, p13, p38, p43-44|Permian|Permian|See also p2, p133-146, p161, p179-187, p195. Previously the Wolverton Adamellite. Named after the Parish of Wolverton. Cape York Peninsula Batholith. These authors propose a type area around MGA 719548 8520080. Resistant; well-exposed. Early Permian. Geophysics, geochemistry well described. Lithology described in great detail; numerous photomicrographs. Most highly-fractionated and evolved granite in the Cape York Peninsula Batholith. Associated with significant alluvial and eluvial tin deposits, but no economically viable lodes have been found. Traces of wolframite reported. Part of Kennedy Igneous Association.|280.4 +/- 1.5 Ma (SHRIMP; Cross et al. in prep.).|Weymouth Supersuite.||Intrudes Morris Granite. Is nonconformably overlain by Gilbert River Formation.|Heterogeneous unit, mainly fine- to medium-grained, uneven-grained to slightly porphyritic, leucocratic granite; tourmaline-bearing leucogranite is a local variant. Massive, non-foliated and relatively undeformed. Joints and quartz veins. I-type.|10-APR-19
20383|Wolverton Granite|71853|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||Pinkish-grey to pale brown, or pale grey, fine- to medium-grained, uneven-grained to slightly porphyritic leucogranite, biotite leucogranite, tourmaline-muscovite leucogranite.|
20383|Wolverton Granite|71854|5|Briefly described|Map legend.|Permian|Permian|||Weymouth Supersuite.|||Pinkish grey to pale brown, or pale grey, fine- to medium-grained, uneven-grained to slightly porphyritic leucogranite, biotite leucogranite, tourmaline-muscovite leucogranite.|
20383|Wolverton Granite|72983|3|Fully described|p4, p7, p48, p56-60|Kungurian|Kungurian|Kennedy Igneous Association. Coen Inlier, northern. Cape York region. Highly fractionated, reduced I-type granite. Associated with significant alluvial and eluvial tin deposits, minor wolframite and rare tantalite, +/- gold; although primary mineralisation is rarely located in situ. Textural, mineralogical, and compositional heterogeneity suggest the unit consists of several discrete phases and/or intrusions. Age is within uncertainty of that of Spion Kop rhyolite, Weymouth Granite and Twin Humps Granite.|280.4 +/- 1.5 Ma SHRIMP U-Pb|||Intrudes Morris Adamellite.|Texturally, mineralogically and compositionally heterogeneous monzogranite to syenogranite. Includes anastomosing networks of open-spaced quartz veins cut by substantial v. felsic dykes.|
20435|Wondoola beds|23425|4|Described|Table 9.7 p393.|||Geological Province Karumba beds.||||||
20435|Wondoola beds|40648|6|Mentioned|p12|||||||||
20435|Wondoola beds|42637|6|Mentioned|p32|||||||||
20435|Wondoola beds|61155|5|Briefly described|p16|Pleistocene|Late Pliocene|Together with Claraville and Armraynald beds thickness is 70m. Geological Province: Western Cape York, Karumba Basin.||||||
20435|Wondoola beds|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Quaternary|Pliocene||||||Red and grey clay, silt, sand|
20435|Wondoola beds|67402|5|Briefly described|p177 tbl CRP/KRM1|Quaternary|Neogene|Karumba Basin. Deposited in a fluvial to paralic environment.||||Unconformably overlies the Wyaaba beds.|Silt, clay, clayey quartzose sand and gravel.|
20435|Wondoola beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit and the Armraynald beds are mapped under the symbol TQ: alluvium and lacustrine deposits.||||||
20435|Wondoola beds|69599|5|Briefly described|p585, p603|Pleistocene|Pliocene|Carpentaria region. Up to 60m thick.||||Correlated with Claraville and Armraynald beds.|Silt, clay, sandy clay and minor sand and gravel.|
20435|Wondoola beds|70354|5|Briefly described|Map legend|Pleistocene|Pliocene||||||Red and grey clay, silt and sand.|
20435|Wondoola beds|70356|5|Briefly described|Map legend.|Pleistocene|Pliocene||||||Red and grey clay, silt and sand.|
20435|Wondoola beds|70570|5|Briefly described|Map legend.|Quaternary|Neogene||||||Red and grey clay, silt and sand.|05-MAY-16
20435|Wondoola beds|70572|5|Briefly described|Map Legend|Quaternary|Neogene||||||Red and grey clay, silt and sand.|20-JAN-22
20435|Wondoola beds|70574|5|Briefly described|Map Legend|Quaternary|Neogene||||||Red and grey clay, silt and sand.|
20435|Wondoola beds|73553|6|Mentioned|p9|Tertiary|Tertiary|Landsborough Graben.||||||
20496|Woodenbong beds|22865|6|Mentioned|Fig22.9 p317|||||||||28-SEP-05
20496|Woodenbong beds|23812|5|Briefly described|p33 Fig.6|||Geological Province: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|40250|6|Mentioned|Fig.7|||||||||
20496|Woodenbong beds|43008|5|Briefly described|map legend|||||||||
20496|Woodenbong beds|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
20496|Woodenbong beds|60281|6|Mentioned|p27|||Replaced Woodenbong Beds. Lithic clastics. Geological Province: Clarence-Moreton Basin.||||||01-NOV-05
20496|Woodenbong beds|60993|3|Fully described|p4, p36|Late Jurassic|Middle Jurassic|Sandstone, siltstone, carbonaceous mudstone and minor coal. Conformably overlie Walloon C.M. Grades laterally into Kanagroo Creek Sandstone and probably Grafton Formation. Max. thickness: ?>400m. Geol. Prov: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|60995|5|Briefly described|p55 Fig. 6|||Interpreted as part of or equivalent to Kangaroo Creek Sst. Massive to medium-bedded, cross-bedded, labile, feldspathic and lesser quartzose sandstone sequence overlying the Walloon Coal. Mes.||||||
20496|Woodenbong beds|60997|5|Briefly described|p139 Fig. 1|Berriasian|Kimmeridgian|Geological Province: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|69594|5|Briefly described|p544|||Clarence-Moreton Basin (QLD only). In NSW the lower part is known as the Kangaroo Creek Sandstone and the upper part is known as the Grafton Formation. >400m thick. Fluvial deposits, sourced from granites of the New England Batholith.||||Conformably overlies Walloon Coal Measures.|Lower part: massive, grey, cross-bedded labile sandstone, ripple-marked siltstone common. Upper part not described: may be similar to Grafton Formation.|
20496|Woodenbong beds|73570|5|Briefly described|p911|||Grades laterally to the southeast into the Kangaroo Creek Sandstone.|||||Feldspathic to lithic sandstones.|
20523|Woodmillar Andesite|24382|5|Briefly described|Map legend|Late Triassic|Late Triassic|Parent: Aranbanga Volcanic Group.||||||18-AUG-08
20523|Woodmillar Andesite|41738|2|Defined|p169|Late Triassic||Reserved as Woodmillar Creek.||||||18-AUG-08
20523|Woodmillar Andesite|41790|5|Briefly described|p474|||||||||
20523|Woodmillar Andesite|42054|6|Mentioned|p272|||||||||
20523|Woodmillar Andesite|63821|5|Briefly described|p21|||Base of the Aranbanga Volcanic Group. Mainly an aphyric or microphyric andesite to basaltic andesite.||||||07-FEB-11
20523|Woodmillar Andesite|68679|5|Briefly described|p437, p439|Late Triassic|Late Triassic|Gayndah region, northern New England Orogen. <20m thick; forms nearly flat benches.||Basal Aranbanga Volcanic Group.||Unconformably overlies Mount Marcella Volcanics. Is overlain by Beeswing Rhyolite and Wetheron Basalt.|Altered microphyric or aphyric andesite to basaltic andesite lava; groundmass characteristically exhibits strong flow-alignment of plagioclase.|
20523|Woodmillar Andesite|73450|5|Briefly described|p30, p34-35|||Lowermost unit of the Aranbanga Volcanic Group.||Aranbanga Volcanic Group|||Basaltic andesite.|
20540|Woogaroo Subgroup|12597|5|Briefly described|p491, |||Of Cranfield and Schwarzbock (1972). Initially for the Ipswich area; extended basin-wide by Wells et al. (1990). Includes also formations previously mapped as Moorooka Formation, Helidon Sandstone and Wivenhoe Sandstone. 150-1120 m thick.||Unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|13516|5|Briefly described|p159 fig 8|Early Jurassic|Late Triassic|From Clarence-Moreton Basin.||Of Bundamba Group||||
20540|Woogaroo Subgroup|22845|6|Mentioned|p76|Jurassic|Triassic|||||||
20540|Woogaroo Subgroup|22857|5|Briefly described|p314, p318 Fig. 22.10A,B|Early Jurassic|Rhaetian|Of the Bundamba Group. Max. thickness: 480m. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|22865|5|Briefly described|p314,Fig22.9p317|||||||||
20540|Woogaroo Subgroup|23435|5|Briefly described|p66|||||||||
20540|Woogaroo Subgroup|23799|3|Fully described|p46, p10 Tb.1|Early Jurassic|Late Triassic|See also p48 Fig. 3. Of the Bundamba Group. Conformably overlain by Marburg Subgroup; unconformably overlies Maronghi Creek beds, Woolshed Mountain Granodiorite and Taron beds. Max. thickness: ~250m. Geological Province: Clarence-Moreton Basin.||||||04-JAN-17
20540|Woogaroo Subgroup|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group.||||||
20540|Woogaroo Subgroup|23811|5|Briefly described|Map Legend|Pliensbachian|Anisian|Of Bundamba Group.  Includes: Nymboida, Red Cliff and Evans Head Coal Measures, Chillingham Volcanics, Laytons Range Conglomerate, Raceview Formation and Ripley Road Sandstone.||||||21-SEP-05
20540|Woogaroo Subgroup|23812|5|Briefly described|p33 Fig.6|||Of Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Bundamba Group.  Quartzose sandstone, siltstone, shale, conglomerate, minor coal (Clarence-Moreton Basin).||||||
20540|Woogaroo Subgroup|36351|6|Mentioned|p373|||||||||
20540|Woogaroo Subgroup|36354|6|Mentioned|p371|||||||||
20540|Woogaroo Subgroup|36579|6|Mentioned|p447|||||||||
20540|Woogaroo Subgroup|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
20540|Woogaroo Subgroup|37375|6|Mentioned|p474|||||||||
20540|Woogaroo Subgroup|37463|6|Mentioned|p479|||||||||
20540|Woogaroo Subgroup|37616|6|Mentioned|p31|||||||||
20540|Woogaroo Subgroup|38307|6|Mentioned|p521|||||||||
20540|Woogaroo Subgroup|38441|6|Mentioned|Map legend|Early Jurassic|Rhaetian|Rhaetian - Early Jurassic||||||
20540|Woogaroo Subgroup|39079|6|Mentioned|p10|||||||||
20540|Woogaroo Subgroup|39445|6|Mentioned|Table 10|||||||||
20540|Woogaroo Subgroup|39907|6|Mentioned|p8|||||||||
20540|Woogaroo Subgroup|39943|6|Mentioned|Table 10A|||||||||
20540|Woogaroo Subgroup|40579|6|Mentioned|Map legend|Early Jurassic|late Rhaetian|||||||
20540|Woogaroo Subgroup|40623|5|Briefly described|p7|||||||||
20540|Woogaroo Subgroup|40780|4|Described|p6|||||||||
20540|Woogaroo Subgroup|41591|6|Mentioned|p17|||||||||
20540|Woogaroo Subgroup|41631|4|Described|p6|||||||||
20540|Woogaroo Subgroup|41906|3|Fully described|Table 2 p15|||||||||02-DEC-13
20540|Woogaroo Subgroup|42248|5|Briefly described|p397|||||||||
20540|Woogaroo Subgroup|42316|6|Mentioned|p7|||||||||
20540|Woogaroo Subgroup|42317|5|Briefly described|p2|||||||||
20540|Woogaroo Subgroup|42319|5|Briefly described|p3|||||||||
20540|Woogaroo Subgroup|42336|5|Briefly described|p4|||||||||
20540|Woogaroo Subgroup|42463|6|Mentioned|Fig.3 P170|||||||||
20540|Woogaroo Subgroup|42869|5|Briefly described|Fig.2 P32|||||||||
20540|Woogaroo Subgroup|42893|6|Mentioned|p8|||||||||
20540|Woogaroo Subgroup|42894|5|Briefly described|Fig.1 P20|||||||||
20540|Woogaroo Subgroup|42951|5|Briefly described|Fig.11|||of Bundamba Group||||||
20540|Woogaroo Subgroup|43008|5|Briefly described|map legend|||||||||
20540|Woogaroo Subgroup|43076|5|Briefly described|p9|||||||||
20540|Woogaroo Subgroup|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
20540|Woogaroo Subgroup|43736|6|Mentioned|p3|||||||||
20540|Woogaroo Subgroup|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Underlies: Gatton Sandstone.  Of the Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
20540|Woogaroo Subgroup|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group. Geological Province: Moreton Basin||||||
20540|Woogaroo Subgroup|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Includes: Ripley Road Sandstone, Raceview Formation.||||||
20540|Woogaroo Subgroup|60281|5|Briefly described|p24, p29, Fig.18 App 1|Late Triassic|Late Triassic|Of the Bundamba Group.  Includes the Ripley Road Sandstone, Raceview Formation and Laytons Range Conglomerate. Overlain by the Gatton Sandstone (Marburg Subgroup).||||||
20540|Woogaroo Subgroup|60993|3|Fully described|p4, p6 Fig. 2|||Oldest part of the Bundamba Group. Comprises: Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone. Replaces the original Bundamba Group division of Tabulum Group of McElroy (1963). Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|60995|4|Described|p51 Fig. 3|Late Triassic|Late Triassic|Basal part of the Bundamba Group. The classic sequence of deposits within this subgroup show considerable variation across the basin.  Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|60997|5|Briefly described|p138, p142 Fig. 4|Sinemurian|Rhaetian|Contains quartzose to quartzo-feldspathic sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2..||||||
20540|Woogaroo Subgroup|60999|5|Briefly described|p164||Late Triassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61002|6|Mentioned|p197|||Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61004|5|Briefly described|p230, p232|Jurassic|Triassic|Of the Bundamba Group. Includes Laytons Range Conglomerate, Raceview Formation and Ripley Road Sandstone. Contains vitrinite-rich coals; minor component is inertinite. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61006|5|Briefly described|p277, p278 Fig. 2|Jurassic|Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61310|5|Briefly described|Table C1 (p22-23)|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|63748|5|Briefly described|p21|||Basal unit of Bundamba Group. Overlain by Marburg Subgroup. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
20540|Woogaroo Subgroup|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Bundamba Group. Includes the Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
20540|Woogaroo Subgroup|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Late Triassic|Clarence-Moreton and Southern Nambour Basins.||Lower unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation, Ripley Road Sandstone, Nambour Formation, and the lower part of the Landsborough Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|67402|6|Mentioned|p187|||Clarence-Moreton Basin.||Bundamba Group|Includes the Aberdare Conglomerate, Laytons Range Conglomerate, Raceview Formation and the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Bundamba Group, the Marburg Subgroup, and Landsborough Sandstone, are all mapped under the symbol, RJb.||Unit in Bundamba Group.||||
20540|Woogaroo Subgroup|68576|5|Briefly described|Q_8B: p11|Jurassic|Triassic|Shorncliffe, western side of Moreton Bay. Fluviatile sediments.||||||
20540|Woogaroo Subgroup|68679|5|Briefly described|p395|||||Bundamba Group.|Aberdare Conglomerate.|Unconformably overlies Ipswich Coal Measures.||
20540|Woogaroo Subgroup|69297|5|Briefly described|p487 fig 5.38|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. More than 480m thick.||Bundamba Group|Includes the Laytons Range Conglomerate, Raceview Formation and the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|69594|4|Described|p519, p543-547, p560-561, p572|Early Jurassic|Rhaetian|Defined by Cranfield and Schwarzbock (1972) after Staines (1964). Clarence-Moreton Basin and southern Nambour Basin. Fluvial to lacustrine deposits. This name replaced the Helidon Sandstone (obsolete; used now only for the building stone quarried at Helidon).||Bundamba Group.|Ripley Road Sandstone, Raceview Formation, Aberdare Conglomerate, Nambour Formation.|Overlies North Arm Volcanic Group. Unconformably overlies Ipswich Coal Measures. Is overlain by Marburg Subgroup. Is intruded by the Brisbane Valley Porphyrites.|A thick succession of mainly conglomerate and sandstone.|
20540|Woogaroo Subgroup|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Triassic|Northern Clarence-Moreton Basin area.||Unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation, Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Bundamba Group.|Raceview Formation, Ripley Road Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|71628|5|Briefly described|p19-147|||Clarence-Moreton Basin.|||Laytons Range Conglomerate.|||
20540|Woogaroo Subgroup|71805|5|Briefly described|p76|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin.||Bundamba Group|Includes the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|72297|5|Briefly described|p724, p726, p748|||Clarence-Moreton Basin. At Ravensbourne, 34km NE of Toowoomba, is associated with kaolin deposits.|||Helidon Sandstone.|Includes/partly equivalent to Landsborough Sandstone.||
20540|Woogaroo Subgroup|72298|6|Mentioned|p802|||Clarence-Moreton Basin. Has supplied small supplies of groundwater for irrigation.||||||
20540|Woogaroo Subgroup|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
20540|Woogaroo Subgroup|73306|5|Briefly described|p566-567, 569|Jurassic|Late Triassic|Clarence-Moreton Basin. It is displaced by steep SW-dipping reverse faults.||Bundamba Group||Is overlain by Marburg Subgroup.||
20601|Woondum Granite|23251|5|Briefly described|Table 5 p33||Late Triassic|Age: K/Ar 223 and 226 Ma. Of the South East Queensland Volcanic and Plutonic Province.  See also p22.||||||21-JUN-06
20601|Woondum Granite|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
20601|Woondum Granite|34573|6|Mentioned|p34|||Middle Triassic||||||
20601|Woondum Granite|35101|3|Fully described|p79|||||||||
20601|Woondum Granite|36926|6|Mentioned|p175|||||||||
20601|Woondum Granite|36954|6|Mentioned|p114|||||||||
20601|Woondum Granite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
20601|Woondum Granite|39261|6|Mentioned|p117|||||||||
20601|Woondum Granite|39445|5|Briefly described|Table 12|||||||||
20601|Woondum Granite|41272|6|Mentioned|M 1of1 C16|||||||||
20601|Woondum Granite|41917|6|Mentioned|p522|||||||||
20601|Woondum Granite|42695|5|Briefly described|Fig.2|Triassic||||||||
20601|Woondum Granite|42751|5|Briefly described|p27|||see also Fig.1 P23||||||
20601|Woondum Granite|43008|5|Briefly described|map legend|||||||||
20601|Woondum Granite|43100|4|Described|p55||Late Triassic|||||||
20601|Woondum Granite|44752|14|Not recorded|p301||Jurassic|||||||
20601|Woondum Granite|44754|14|Not recorded|p5,10,Fig.1||Jurassic|||||||
20601|Woondum Granite|44928|5|Briefly described|Map Legend||Late Triassic|||||||
20601|Woondum Granite|48894|6|Mentioned|p41|||Age. ?Triassic or Jurassic||||||
20601|Woondum Granite|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Granite, adamellite, granodiorite, quartz diorite.||||||15-JUL-04
20601|Woondum Granite|67203|6|Mentioned|p3|Triassic|Triassic|||||||
20601|Woondum Granite|68679|5|Briefly described|p370, p428-429, p472|Late Triassic|Late Triassic|Northern New England Orogen; Gympie area. Is mentioned as separating two differing structural domains within the Kin Kin beds.|225.7 Ma and 222.6 Ma (Webb and McDougall, 1967).|||Intrudes the Cedar Pocket Porphyry.|Includes four mappable phases. Coarse-grained, equigranular granite is dominant; monzodiorite (in the NE), a microgranite rim (in the NW) adjacent to a plateau of porphyritic dacite that may be the oldest phase.|
20617|Woorim beach sand|38302|6|Mentioned|Table 1|||Informal name||||||
20617|Woorim beach sand|39495|6|Mentioned|p142|||||||||
20617|Woorim beach sand|62102|5|Briefly described|p367 Tb. 1|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast - forms a strandplain.  Age: 125Ka.||||||09-MAY-06
20633|Worthington beds|39445|6|Mentioned|p169|||||||||
20645|Wreath Member|24393|5|Briefly described|p151 Fig. 7|Mesozoic|Mesozoic|Fluvial deposits.  Of the Garraway Sandstone.||||||08-APR-13
20645|Wreath Member|42061|5|Briefly described|Fig.4 P151|||||||||
20645|Wreath Member|62837|5|Briefly described|Stratigraphic columns|Tithonian|Oxfordian|Of the Garraway Formation. Age: ~151-140Ma.  Geological Province: Northern Cape York.||||||01-MAR-10
20690|Wyaaba beds|23425|4|Described|p393 Table 9.7.|||Geological Province Karumba Basin. Max thickness: 150 m.||||||
20690|Wyaaba beds|23430|5|Briefly described|p526|||||||||
20690|Wyaaba beds|23496|5|Briefly described|Table 4, p61|Early Pliocene|Miocene|~60m thick. Was mapped as Bulimba Formation previously.||||||
20690|Wyaaba beds|40648|6|Mentioned|p13|||||||||
20690|Wyaaba beds|42637|4|Described|p31|||||||||
20690|Wyaaba beds|43287|5|Briefly described|Map Legend||Neogene|||||||
20690|Wyaaba beds|45145|6|Mentioned|Fig.18|||||||||
20690|Wyaaba beds|47083|5|Briefly described|p20|Pliocene|Miocene|||||||
20690|Wyaaba beds|61155|5|Briefly described|p16|?Late Miocene|Middle Miocene|Together with Falloch beds overlie Carl Creek and Gregory Downs Limestones. Together with Falloch beds thickness is 140m. Geological Province: Western Cape York, Karumba Basin.. See also p4, p5.||||||
20690|Wyaaba beds|64820|5|Briefly described|pS6 Fig. 4, pS7, pS11|Neogene|Neogene|Limestone, sandstone, siltstone (mainly offshore). Geological province: Weipa Sub-basin, Carpentaria Basin. Also written as "Wyaaba beds" (of the Karumba Basin).||||||
20690|Wyaaba beds|67402|5|Briefly described|p176, p180, p181 tbl CRP/KRM2, p239|Cheltenhamian|Bairnsdalian|Karumba Basin. Aquifers are present in this formation. Deposited in a fluvial to paralic environment. Approximately 90m thick. Unsuitable reservoir for the storage of carbon dioxide.||||Unconformably overlies the Gregory Downs and Carl Creek Limestones. Overlain by the Claraville, Wondoola and Armraynaid beds.|Clayey quartzose sand, sandstone, conglomerate and clayey calcareous siltstone.|
20690|Wyaaba beds|68553|6|Mentioned|Map legend|Neogene|Neogene|This unit, as well as the Falloch, Lilyvale and Yam Creek beds, are all mapped under the symbol, Tu.||||||
20690|Wyaaba beds|69599|5|Briefly described|p585, p602-603, p651|Miocene|Miocene|Carpentaria region. Erosion and laterisation produced the Pliocene Kendall Surface.||||Conformably overlies the Bulimba Formation. Correlated with Yam Creek, Lilyvale and Falloch beds, and Darai Limestone.|Onshore, up to 150m of clay-rich quartzose sandstone, conglomerate, sandy claystone and calcareous siltstone; offshore, up to 140m of limestone, calcrete and calcarenite.|
20690|Wyaaba beds|71792|6|Mentioned|BD|||Considered to be equivalent to the Lilyvale, Falloch and Yam Creek beds.||||Conformably overlies the Bulimba Formation.||
20690|Wyaaba beds|71854|5|Briefly described|Map legend.|Pliocene|Miocene||||||Clayey quartzose sand and sandstone, granule to (locally) pebble gravel, conglomerate; interbedded sandy clay and calcareous mudstone.|
20695|Wyandra Sandstone Member|12597|5|Briefly described|p492 Tb.1, p499|Barremian|Early Cretaceous|E Eromanga Basin. Up to 60m thick. Forms the youngest pressurised aquifer in the Basin.||Unit in Cadna-owie Formation.|||Fine- to coarse-grained quartzose to sub-labile sandstone, pebbly in part, generally well sorted, porous and permeable; with minor siltstone interbeds towards the top.|
20695|Wyandra Sandstone Member|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Cadna-owie Formation||||
20695|Wyandra Sandstone Member|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Bulldog Shale, underlying unit is Murta Formation, parent is Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|22912|5|Briefly described|33|||Geol province Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|23375|4|Described|Fig2 p265,267,269,271,277,279|Barremian|Hauterivian|Of the Cadna-owie Formation. In the Eromanga Basin.||||||17-JAN-08
20695|Wyandra Sandstone Member|23430|4|Described|p524 Table 14.7|||Of Cadna-owie Formation. Eromanga Basin Province.||||||
20695|Wyandra Sandstone Member|23982|5|Briefly described|p57|Cretaceous|Jurassic|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||18-JUL-14
20695|Wyandra Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24482|5|Briefly described|p44|Cretaceous|Jurassic|Of the Cadna-owie Formation. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|32314|6|Mentioned|Fig. 4|||||||||
20695|Wyandra Sandstone Member|33017|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|33075|2|Defined|p452|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|35239|6|Mentioned|p265|||||||||
20695|Wyandra Sandstone Member|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
20695|Wyandra Sandstone Member|36251|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|36571|6|Mentioned|Table 4|||||||||
20695|Wyandra Sandstone Member|38226|6|Mentioned|Table 1|||See also Fig.6.||||||
20695|Wyandra Sandstone Member|39070|4|Described|p364|||||||||
20695|Wyandra Sandstone Member|39211|5|Briefly described|Fig.3|||See also Fig.4||||||
20695|Wyandra Sandstone Member|39478|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|39480|6|Mentioned|p196|||||||||
20695|Wyandra Sandstone Member|39481|6|Mentioned|p181|||||||||
20695|Wyandra Sandstone Member|39846|6|Mentioned|p48|||||||||
20695|Wyandra Sandstone Member|39847|5|Briefly described|p38|||||||||
20695|Wyandra Sandstone Member|39989|4|Described|p423|||||||||
20695|Wyandra Sandstone Member|40199|4|Described|p25|||||||||
20695|Wyandra Sandstone Member|40249|6|Mentioned|p41|||||||||
20695|Wyandra Sandstone Member|40681|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|40687|3|Fully described|p417|||||||||
20695|Wyandra Sandstone Member|40832|6|Mentioned|p457|||||||||
20695|Wyandra Sandstone Member|40910|6|Mentioned|Table 3|||||||||
20695|Wyandra Sandstone Member|40926|6|Mentioned|Table 2|||||||||
20695|Wyandra Sandstone Member|41064|6|Mentioned|p62|||||||||
20695|Wyandra Sandstone Member|41089|6|Mentioned|p156|||||||||
20695|Wyandra Sandstone Member|41097|6|Mentioned|p165|||||||||
20695|Wyandra Sandstone Member|41165|5|Briefly described|p360|||||||||
20695|Wyandra Sandstone Member|41177|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|41183|6|Mentioned|p310|||||||||
20695|Wyandra Sandstone Member|41186|5|Briefly described|p200|||||||||
20695|Wyandra Sandstone Member|41198|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|41219|6|Mentioned|p334|||||||||
20695|Wyandra Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
20695|Wyandra Sandstone Member|41286|6|Mentioned|p117|||||||||
20695|Wyandra Sandstone Member|41523|5|Briefly described|p271|||||||||
20695|Wyandra Sandstone Member|41681|6|Mentioned|p23|||||||||
20695|Wyandra Sandstone Member|41724|6|Mentioned|p382|||||||||
20695|Wyandra Sandstone Member|42067|5|Briefly described|p313|||||||||
20695|Wyandra Sandstone Member|42084|6|Mentioned|Fig.3 P356|||||||||
20695|Wyandra Sandstone Member|42085|6|Mentioned|Fig.2 P374|||||||||
20695|Wyandra Sandstone Member|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
20695|Wyandra Sandstone Member|43105|5|Briefly described|Fig.9,p15.|||Of Cadna-owie Formation.||||||16-SEP-08
20695|Wyandra Sandstone Member|43122|5|Briefly described|p23|||of Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|43602|5|Briefly described|203|||In Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|44133|6|Mentioned|p115|||||||||
20695|Wyandra Sandstone Member|46791|6|Mentioned|Table 1|||See also Fig.7||||||
20695|Wyandra Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20695|Wyandra Sandstone Member|46939|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation. Overlain by Wallumbilla Formation and partly by Bulldog Shale. Geological Province: Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|61014|5|Briefly described|pp532-554. |Lower Cretaceous|Lower Cretaceous|Eromanga Basin. The uppermost oil reservoir in the Eromanga Basin succession in south-west Queensland. Trace fossils (burrows) occur throughout. A regressive-transgressive sequence of fluvial, overbank crevasse-splay, mouth bar, estuarine and distal distributary channel deposits. Grain-size analysis and sequence-stratigraphic analogues are detailed.||Unit in Cadna-owie Formation.|||An amalgamation of fining-upward sandstone units to 2 m thick, with ripple cross-lamination, flaser bedding and multiple layers of carbonaceous detritus; commonly capped by thin mudstone units; interbedded mudstone and thin coal; bioturbated at top.|
20695|Wyandra Sandstone Member|61312|5|Briefly described|p64|Early Cretaceous|Early Cretaceous|Uppermost part of the Cadna-owie Formation. Dominantly sandstone; may contain reservoir quality sands. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20695|Wyandra Sandstone Member|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Of the Cada-owie Formation. Geological Province: Eromanga Basin.||||||21-APR-08
20695|Wyandra Sandstone Member|63979|5|Briefly described|p46, Fig. 44|Barremian|Hauterivian|Of (upper) Cadna-owie Formation occupying same stratigraphic position in Qld. as Mount Anna Sandstone in SA. A major aquifer in Great Artesian Basin. Geological province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|64048|5|Briefly described|p71, p72|||Of the Cadna-owie Formation. Records high oil flow rates.||||||07-FEB-11
20695|Wyandra Sandstone Member|64197|6|Mentioned|p625 Fig.1c|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Cadna-owie Formation.||Is overlain by Bulldog Shale or Wallumbilla Formation.||
20695|Wyandra Sandstone Member|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Overlain by Wallumbilla Formation and Bulldog Shale.||||||08-MAR-12
20695|Wyandra Sandstone Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Cadna-owie Formation.||||
20695|Wyandra Sandstone Member|66623|3|Fully described|p239, p243, pp254-255.|Early Cretaceous|Early Cretaceous|Equivalent to the informal Mokely Creek Sandstone member (Morton 1982), and topmost Gum Vale Beds. Glacial dropstones preserved towards the top. A widespread marker unit in Tibooburra-Milparinka area. Thickness to 20 m. Similar fossil assemblage as Cadna-owie Formation. Upper boundary is strongly diachronous, younging towards basin margins.||Unit in Cadna-owie Formation.||Is conformably, but sharply overlain by Wallumbilla Formation (or, in SA, by Bulldog Shale).|Calcareous quartzose sandstone, pebbly sandstone and quartz pebble conglomerate; exotic lonestone cobbles and boulders of quartz-veined quartzite and felsic volcanic lithologies common throughout.|05-JUN-13
20695|Wyandra Sandstone Member|66915|4|Described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Eromanga Basin. Abbreviated as Wyandra Sandstone in some figures and text. See also parent Cadna-owie in this paper.||Uppermost unit of Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||12-JAN-17
20695|Wyandra Sandstone Member|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate; local ferruginous, coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.||Overlies Namur Sandstone.|Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67323|5|Briefly described|p87|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|67402|4|Described|p26, p26 tbl RRM4|Aptian|Aptian|Eromanga Basin. Maximum thickness of <10m. Deposited as beach sands during a marine transgressive cycle. Minor hydrocarbon reservoir but may be a major carbon dioxide storage reservoir. See also p43 tbl HPB1, p108, p109, p115, p121, p303.||Cadna-owie Formation.||Overlies the Lower Cadna-owie Formation. Overlain by the Wallumbilla Formation.|Mainly fine to medium-grained, thickly bedded sandstone with minor siltstone at the top.|
20695|Wyandra Sandstone Member|67561|5|Briefly described|p51, p52 Fig.2, p53, p64, p65, p67|Barremian|Valanginian|Eromanga Basin. Australian Spore-Pollen zonation: C.wonthaggiensis. Occurs at the top of the Cadna-Owie Formation. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||Of the Cadna-Owie Formation.||Overlain by the Bulldog Shale.|Coarse-grained sandstone.|20-JAN-17
20695|Wyandra Sandstone Member|68731|6|Mentioned|pp209-211|||||||||
20695|Wyandra Sandstone Member|69457|5|Briefly described|p41:3, 7|Early Cretaceous|Early Cretaceous|Senior et al. (1975). Eromanga Basin. Transitional (?beach setting) deposits.||Cadna-owie Formation.||Stratigraphic equivalent to Wyandra Sandstone Member (in Qld).||12-JUL-16
20695|Wyandra Sandstone Member|69594|5|Briefly described|p519, p526-528|Aptian|Barremian|Eromanga Basin. 3-18m thick. An important regional aquifer. A prominent regional marker. Beach deposits.||Topmost Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation)..|Coarse, sporadically pebbly, quartzose to sublabile sandstone.|
20695|Wyandra Sandstone Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Cadna-owie Formation||Overlain by Doncaster Member||
20695|Wyandra Sandstone Member|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Wyandra Sandstone Mbr.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|69946|3|Fully described|p19-21, p57, p94|Early Cretaceous|Early Cretaceous|Eromanga Basin. Defined in the subsurface in Qld (Senior et al., 1975) as the upper sandy part of the Cadna-owie Formation. Type section is the interval 357 - 373m in Water Bore No. 2049 (Queensland Irrigation and Water Supply records), 15km SE of Wyandra. Proposal for a new type section discussed. Can be correlated on wireline logs into the Cooper region in SA. 3-18m thick in Qld (subsurface). Wireline log correlations.||Uppermost unit in Cadna-owie Formation.||Is overlain conformably by Bulldog Shale or Wallumbilla Formation.|Medium- to coarse-grained, quartzose to labile sandstone with scattered pebbles. Locally contains up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|69947|5|Briefly described|p9, p13 Fig.7.2, p31-32 Figs.7.20-21|Early Cretaceous|Early Cretaceous|Lang et al. (2001). Eromanga Basin. Basal regional sequence boundary, overlain by amalgamated fluvial distributary channel fill. Appears simply as Wyandra Sandstone in Fig.7.20. Generalised stratigraphic log showing key surfaces and systems tracts.||Cadna-owie Formation||Is overlain by Bulldog Shale and the Wallumbilla Formation.|Basal in-filled fluvial channel sediments overlain by tidally-influenced sediments followed by heterolithic marine strata.|07-FEB-18
20695|Wyandra Sandstone Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse-grained, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70821|4|Described|p21 Fig.2.6, p22, p33, p79-80,p82,p85-86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Typically 3-18m thick; locally considerably thicker. Historically considered a beach deposit; more recent work suggests it may well be an impact tsunami deposit formed by the Tookoonooka impact event to the NE of the project area (Bron, 2009). Hydrochemistry mentioned, hydrostratigraphic properties. Aquifer: generally artesian.||Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation).|Coarse, sporadically pebbly, quartzose to sub-labile sandstone. Locally with dark carbonaceous laminae.|
20695|Wyandra Sandstone Member|71251|4|Described|p8, p11, p13, p15, p17, p19-20, p29|||See also p48-49, p51. Eromanga Basin. 30m total thickness in Eulo 1 borehole. An aquifer. Natural gamma, magnetic susceptibility data tabulated. Abbreviated in text to Wyandra Sandstone or simply Wyandra. Conductivity diagram.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.|Fine- to medium-grained sandstone, subangular quartz, feldspar and lithic fragments.|
20695|Wyandra Sandstone Member|71342|4|Described|Ch5 p19-p21, Ch5 p57, Ch6 p7|Aptian|Barremian|This unit was first defined by Senior et al (1975) as the upper sandy part of the Cadna-owie Formation. An initial type section was nominated by Senior et al (1975) however, Green, Brain et al (1989) proposed that a new type section was necessary if the original concept of Senior et al was to continue. This unit ranges between 3 and 18m thick in Queensland. Spore-pollen zone is given in Ch5 p57. Hosts commercially producible oil in Aldinga 1. Seal and reservoir characteristics discussed in Ch11. See also  Ch7 p9, Ch7 p11, Ch7 p13, Ch7 p32, Ch11 p2, Ch11 p5, Ch12 p3.||Cadna-owie Formation||Conformably overlain by the Wallumbilla Formation or the Bulldog Shale.|Medium to coarse-grained, quartzose to labile sandstone with scattered pebbles. Sandstones may contain up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|71863|6|Mentioned|p5|Aptian|Aptian|Eromanga Basin.||Cadna-owie Formation||Overlain by the Doncaster Member.||
20695|Wyandra Sandstone Member|71864|6|Mentioned|p13-p14, p17, p26|||Waterbores are reported to intersect this unit which is a moderately producing aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|72297|5|Briefly described|p743|||Eromanga Basin. High oil flows recorded at Talgeberry.||||||
20695|Wyandra Sandstone Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||Cadna-owie FZ.||Is overlain by Doncaster Member (Wallumbilla FZ).||
20695|Wyandra Sandstone Member|72914|5|Briefly described|p14-16, p18, p20-21, p27, p29-30, App.I|Cretaceous|Cretaceous|Major groundwater source in the local region; supplies fresh to slightly brackish water. Natural gamma emissions are very subdued, indicating the quartz-rich nature of the unit. See also accidental misspelling Wyandra Sandstone member p20.||Cadna-owie Formation||Overlain by the Wallumbilla Formation.|Clean quartz sandstone; quartzose and labile lithic gravels.|
20695|Wyandra Sandstone Member|72915|6|Mentioned|p27|Mesozoic|Mesozoic|Constitutes a local aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains oil and gas.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Deltaic shoreface marine depositional environment.|ca 125 Ma|Cadna-owie Formation||Overlies Cadna-owie Formation||
20722|Wynyard Metamorphics|22557|6|Mentioned|p567,569|||||||||
20722|Wynyard Metamorphics|23078|5|Briefly described|p708|||||||||
20722|Wynyard Metamorphics|23854|5|Briefly described|p857|Neoproterozoic|Neoproterozoic|Of Anakie Metamorphic Group. Geological Province: Anakie Inlier.||||||18-JUL-14
20722|Wynyard Metamorphics|24599|5|Briefly described|p499|Neoproterozoic|Neoproterozoic|Geological Province: New England Orogen.||||||
20722|Wynyard Metamorphics|42747|5|Briefly described|p33, Fig.3|||of Anakie Metamorphic Group. Reserved as Wynyard Granodiorite.||||||
20722|Wynyard Metamorphics|43204|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Neoproterozoic or Early Cambrian. Anakie Inlier.||||||23-DEC-11
20722|Wynyard Metamorphics|43213|3|Fully described|p8, p20-22, p39-41, p236|||Named after Wynyard Holding. Structurally highest unit in Anakie Metamorphic Group. Crops out in extreme west of Anakie Inlier. Type area and geophysical properties described.||Unit in Anakie Metamorphic Group.||Structurally overlies Monteagle Quartzite. Is overlain unconformably by Silver Hills Volcanics.|Psammopelitic unit containing grey, originally more labile meta-arenite and biotite-rich schist; locally contains staurolite, andalusite and garnet porphyroblasts.|
20722|Wynyard Metamorphics|43861|2|Defined|25; Fig1p26; p29,30|Late Cambrian|Early Cambrian|In Anakie Metamorphic Group.||||||23-JUN-15
20722|Wynyard Metamorphics|66851|6|Mentioned|p915, 917.|||Bedding is defined by alternating psammitic and schist layers.||Unit in Anakie Metamorphic Group.||||18-JAN-17
20722|Wynyard Metamorphics|68412|5|Briefly described|Map legend|Early Cambrian|Neoproterozoic|Anakie Province.||Unit in Anakie Metamorphic Group.||Conformably overlies Monteagle Quartzite.|Fine-grained mica schist, locally with andalusite porphyroblasts and grey fine-grained foliated quartzite and labile meta-arenite.|
20722|Wynyard Metamorphics|68482|5|Briefly described|Map Legend|Early Cambrian|Neoproterozoic|Anakie Province.||Of the Anakie Metamorphic Group.||Conformably underlain by the Monteagle Quartzite.|Fine-grained mica schist, locally with andalusite porphyroblasts and grey fine-grained foliated quartzite and labile meta-arenite.|
20722|Wynyard Metamorphics|68731|5|Briefly described|p122, p127, p133, p134|Series 2|Neoproterozoic|Anakie Province. Constrained by the youngest significant peak of detrital zircon ages from a pelitic schist sample(Fergusson et al. 2001, 2007a)|600-510 Ma, detrital zircon U-Pb|Of the Anakie Metamorphic Group.||Underlain by the Monteagle Quartzite.|Comprises mica and psammitic schist and has minor quartzite. The rocks are grey and composed of quartz, muscovite, biotite, and secondary chlorite. Porphyroblasts include chlorite, biotite, garnet, and less commonly, staurolite and andalusite.|
20722|Wynyard Metamorphics|68900|5|Briefly described|p6|||Drummond Basin.||||Overlies the Monteagle Quartzite.|Psammopelitic rocks including meta-arenite and biotite-rich schist.|
20722|Wynyard Metamorphics|69541|5|Briefly described|p645 Fig.1(b), p654|Cambrian|Cambrian|||Unit in Anakie Metamorphic Group.|||Psammopelitic schists.|
20722|Wynyard Metamorphics|69952|5|Briefly described|p4|||Maximum depositional age.|c.510 Ma (Fergusson et al., 2001).|Unit in Anakie Metamorphic Group.||||
20722|Wynyard Metamorphics|70033|5|Briefly described|p4|||Thomson Orogen. Maximum depositional age: mid- to late Cambrian.|~510 Ma, Fergusson et al. 2001|Anakie Metamorphic Group||||
20722|Wynyard Metamorphics|70125|5|Briefly described|p394, p408|Middle Cambrian|Middle Cambrian|Probability density plot of U-Pb ages of detrital zircons is compared with that of other units. This ~505 Ma age is from metamorphism at 510-500 Ma (whole-rock K-Ar: Jell, 2013) and age of youngest detrital zircons (510 Ma).|~505 Ma.||||Protoliths of dominantly shale, quartz and lithic sandstone, with minor limestone and mafic volcanics.|
20722|Wynyard Metamorphics|70744|5|Briefly described|p939, p943|||Southern Anakie Province. Detrital zircon and monazite have a prominent source aged 600-510 Ma (Pacific-Gondwana signature).|c.510-500 Ma (estimated from Fig.7).||||Includes lithic psammitic schist.|
20722|Wynyard Metamorphics|70749|5|Briefly described|p42-44, p49, p51|Cambrian|Cambrian|Characterised by abundant 650-500 Ma zircons with a subordinate 1300-900 Ma group, and a maximum depositional age of 511-495 Ma. Zircons sourced from rift-related and back-arc volcanism of the active Gondwana margin.|~510 Ma (maximum depositional age).|Anakie Metamorphic Group (upper part).||||
20722|Wynyard Metamorphics|71966|6|Mentioned|p990|Cambrian|Cambrian|Geological province: Anakie Province, Thomson Orogen.|<510 Ma|||||
20722|Wynyard Metamorphics|73147|6|Mentioned|p144|||Anakie Inlier. Contains detrital zircons with a minor c.1300-900 Ma Grenville Orogen signature.||||||
20722|Wynyard Metamorphics|73425|6|Mentioned|p16|Late Cambrian|Middle Cambrian|Anakie Province, northeast Thomson Orogen.||||||
20722|Wynyard Metamorphics|73600|6|Mentioned|p203|||Anakie Province. Characterised by the Pacific-Gondwanan detrital zircon ages.||||||
20740|Yackah beds|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Cherty dolomite with columnar stromatolites, sandstone, siltstone. Overlies Mount Dobbie Granite.||||||20-DEC-06
20740|Yackah beds|22589|6|Mentioned|p128||Neoproterozoic|||||||
20740|Yackah beds|22907|6|Mentioned|41|||Geological Province: Georgina Basin.||||||11-JUN-08
20740|Yackah beds|23557|6|Mentioned|p98|||Geological Province: Georgina Basin.||||||
20740|Yackah beds|37929|5|Briefly described|p526|||||||||
20740|Yackah beds|39340|6|Mentioned|p359|||||||||
20740|Yackah beds|40538|5|Briefly described|Map legend|Adelaidean|Adelaidean|Sandstone; granule conglomerate; dolostone. Geological Province: Georgina Basin.||||||15-NOV-05
20740|Yackah beds|40906|6|Mentioned|p18|||||||||
20740|Yackah beds|42775|5|Briefly described|p322|||||||||
20740|Yackah beds|45155|6|Mentioned|Fig.7|||In the Georgina Basin.||||||20-DEC-06
20740|Yackah beds|48990|2|Defined|p15|Adelaidean|Adelaidean|||||||
20740|Yackah beds|49027|6|Mentioned|p2|||||||||
20740|Yackah beds|60122|5|Briefly described|p9, p11 Tb. 1|||In Supersequence 1 on HAY RIVER and HUCKITA; not in TOBERMORY sheet. Disconformably overlain by Yardida Tillite. Geological Province: Georgina Basin.||||||
20740|Yackah beds|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Underlies Mount Cornish Formation. Geological province: Georgina Basin.  Sandstone, granule conglomerate, dolomite.||||||20-DEC-06
20740|Yackah beds|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Chertified dolostone, sandstone and siltstone.||||||25-NOV-04
20740|Yackah beds|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Plenty Group. Chertified dolostone, sandstone and siltstone.  Geological Province: southern Georgina Basin.||||||11-OCT-05
20740|Yackah beds|62453|6|Mentioned|p16|||Geological Province: Georgina Basin.||||||
20740|Yackah beds|63450|5|Briefly described|p78 Fig. 5, p79|Neoproterozoic|Neoproterozoic|Disconformably overlain by Yardida Tillite. Geological province: Georgina Basin, West Toko Syncline. Comprise chertified dolostone, sandstone and siltstone; contain a stromatolite in common with Bitter Springs Formation.||||||07-FEB-11
20740|Yackah beds|63562|5|Briefly described|p338 fig 3, p342, p352 fig 10|Cryogenian|Neoproterozoic|Of Georgina Basin.|||||Basal sandstone overlain by a relatively thin carbonate unit.|08-DEC-17
20740|Yackah beds|64068|4|Described|p44, p164, p35, p223|Cryogenian||Lower siliciclastic rocks correlated with Amesbury Quartzite, Heavitree Quartzite, Vaughan Springs Quartzite; upper stromatolitic carbonate correlated with Bitter Springs Formation, Albinia Formation.||Of Plenty Group.||Overlies Mount Dobbie and Jervois Granites. Is disconformably overlain by Yardida Tillite and Mount Cornish Formation.|Interbedded fine to very coarse, grey arkose, sandstone and laminated anoxic shale overlain by stromatolitic dolostone.|05-APR-12
20740|Yackah beds|64793|6|Mentioned|p293|||Georgina Basin. Hosts Acaciella australica Stromatolite Assemblage.||||||
20740|Yackah beds|65363|6|Mentioned|p11.|||Presence of Acaciella australica Stromatolite Assemblage in the Woolnough Member of the Browne Formation enables correlation with this unit, Skates Hill Formation, Loves Creek Member of the Bitter Springs Formation, and Coominaree Dolomite.||||||
20740|Yackah beds|65366|5|Briefly described|p24|||Georgina Basin.  Includes the Acaciella australica Stromatolite Assemblage||||||
20740|Yackah beds|67870|6|Mentioned|p43|Neoproterozoic|Neoproterozoic|Georgina Basin.||||||
20740|Yackah beds|68270|5|Briefly described|p680,683|Tonian|Tonian|Southern Georgina Basin.||||Overlain disconformably by Mount Cornish Formation and Yardida Tillite.||
20740|Yackah beds|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SE Georgina Basin, Centralian A Superbasin. Supersequence 1.||Plenty Group.||||12-JUL-16
20740|Yackah beds|69443|4|Described|p28:5-8|Cryogenian|Cryogenian|Walker (1980). Informal name. Southern Georgina Basin. Up to 250m thick. Poorly exposed. Dominantly fluviatile, minor intertidal to very shallow-marine deposits in the lower interval; partially emergent, metahaline-hypersaline lacustrine to anoxic deep marine conditions in upper interval.||Plenty Group.||Is overlain disconformably by Yardida Tillite and Mount Cornish Formation. Lower and upper intervals are correlated with Heavitree and Amesbury Quartzites and Bitter Springs Formation respectively.|Interbedded, fine to very coarse (to granule) arkose, sandstone and laminated shale; overlain by or interbedded with an upper interval of silicified, locally stromatolitic (Acaciella australica) dolostone.|12-JUL-16
20740|Yackah beds|69673|6|Mentioned|p112, p114 fig 92|||Up to 250m thick.||Plenty Group|||Interbedded sandstone, laminated shale and silicified, locallly stromatolitic dolostone.|
20740|Yackah beds|72375|5|Briefly described|p5|||Of SE Georgina Basin.||||Equivalent to Heavitree Formation.||
20740|Yackah beds|72516|3|Fully described|p13-15, p64, p85-86, p88, p154, p218|Tonian|Tonian|Georgina Basin. First described in HAY RIVER map sheet. These are the oldest Georgina Basin rocks in the map sheet area. Appears as Yackah Beds on p14 , Yakah beds p13, p15 (misspelling). Subdivided into an upper and lower interval. 26m thick in the map sheet area, 250m thick in HAY RIVER map sheet. The lower interval was deposited in a fluviatile and minor intertidal to very shallow marine environment. The upper interval was deposited in a metahaline-hypersaline lacustrine to anoxic deep marine environment. Contains rare columnar,branching stromatolites in the upper interval. Age correlative of the Vaughan Springs Quartzite in the Ngalia Basin.||Plenty Group||Disconformably overlain by the Mount Cornish Formation. Unconformably overlies the Tarlton Granite and the Denara Orthogneiss. Equivalent to the Heavitree Formation.|Fine- to very coarse-grained subarkose to arkosic granule conglomerate grading upwards into quartz arenite to lithic greywacke and laminated shale. Thinly bedded, lenticular, silicified, yellow, pink and grey dolostone.|04-JUL-22
20740|Yackah beds|73086|6|Mentioned|p18, p30, p39|||Georgina Basin. Deposited in a hypersaline lacustrine to anoxic, deep marine conditions (Walter and Veevers, 1997). [Misspelt as Yakah beds on p9 and p145].||||Correlates to Heavitree Formation.||
20786|Yamahra Conglomerate|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
20786|Yamahra Conglomerate|40896|6|Mentioned|p51|||||||||
20786|Yamahra Conglomerate|44778|14|Not recorded|p129||Late Triassic|||||||
20786|Yamahra Conglomerate|44779|2|Defined|p262-263|||Unconformably overlies Mount Barney Beds.||||||
20786|Yamahra Conglomerate|48917|4|Described|p10|||||||||
20828|Yankee Jack dune sand|38302|6|Mentioned|Table 1|||Informal name||||||
20828|Yankee Jack dune sand|39495|6|Mentioned|p142|||||||||
20828|Yankee Jack dune sand|62102|5|Briefly described|p367 Tb. 1, p370|Pleistocene|Pleistocene|Informal name for morphostratigraphic unit on southeast Queensland coast .  Age: 368Ka. See also p371.||||||09-MAY-06
20834|Yappar Member|9528|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation. Clayey quartz sandstone and minor lithic-quartz sandstone, commonly ferruginised; pebbly in places.||||||08-JUL-15
20834|Yappar Member|9531|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Quartzose sandstone, siltstone, shale.||||||02-JUL-04
20834|Yappar Member|23032|5|Briefly described|p47||Late Jurassic|||||||
20834|Yappar Member|23291|4|Described|81 Tb. 3.6p|Early Cretaceous|Late Jurassic|Parent: Gilbert River Formation. Thickness: up to 30m in Gilberton Plateau. Overlies the Eulo Queen Group. Geological Province: Georgetown Region.||||||08-JUL-15
20834|Yappar Member|23425|4|Described|Table 9.7 p394.|||Of Gilbert River Formation. Carpentaria Basin Province.||||||08-JUL-15
20834|Yappar Member|23496|5|Briefly described|Table 4, p59|Early Cretaceous|Late Jurassic|of Smart and Others 1971. of Gilbert River Formation. ~70m thick.||||||
20834|Yappar Member|23500|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of Gilbert River Formation, Carpentaria and Karumba Basins. Age shown as Late Jurassic? - Early Cretaceous.||||||
20834|Yappar Member|23510|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|of Gilbert River Formation.||||||
20834|Yappar Member|23616|5|Briefly described|Table 1C p12|Early Cretaceous|Late Jurassic|Unconformably overlies Proterozoic metamorphics and granitoids of the Dargalong Inlier, Silurian granitoids of the Blackman Gap Supersuite, and Carboniferous granitoids and felsic volcanics of the Scardons Volcanic Group. Of Gilbert River Formation.||||||
20834|Yappar Member|23713|5|Briefly described|p76 Appendix 2|||Of Gilbert River Formation||||||
20834|Yappar Member|24073|5|Briefly described|p378 Table 2|||Of the Gilbert River Formation.  Maximum thickness: 35m.  Geological Province: Carpentaria Basin.||||||
20834|Yappar Member|24485|3|Fully described|p37, p38 Tb.6|Early Cretaceous|Late Jurassic|Overlying Unit: Coffin Hill Member. Parent: Gilbert River Formation. Max Thickness: ~70m. Geological Province: Carpentaria Basin.||||||08-JUL-15
20834|Yappar Member|24486|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.  Geological Province: Carpentaria Basin.||||||
20834|Yappar Member|30020|6|Mentioned|p29|||||||||
20834|Yappar Member|30584|4|Described|Table 1|||||||||
20834|Yappar Member|30585|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous.||||||
20834|Yappar Member|31168|5|Briefly described|p11|||See also Table 2.||||||
20834|Yappar Member|33176|6|Mentioned|p172|||Re-identification||||||
20834|Yappar Member|33179|4|Described|Table 2|||||||||
20834|Yappar Member|33180|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Upper Jurassic-Lower Cretaceous||||||
20834|Yappar Member|33182|5|Briefly described|p190|||U.Jur.- L.Cret.||||||
20834|Yappar Member|33183|2|Defined|p232|Early Cretaceous|Late Jurassic|Upper Jurassic - Lower Cretaceous||||||
20834|Yappar Member|33528|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic - Early Cretaceous||||||
20834|Yappar Member|35220|6|Mentioned|p16|||||||||
20834|Yappar Member|35811|5|Briefly described|p563|||||||||
20834|Yappar Member|36216|6|Mentioned|p211|||||||||
20834|Yappar Member|37608|3|Fully described|Table 2|||||||||
20834|Yappar Member|39211|6|Mentioned|p36|||Fig.22||||||
20834|Yappar Member|39917|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic-Early Cretaceous||||||
20834|Yappar Member|40218|6|Mentioned|Map legend|Early Cretaceous|Late Jurassic|Late Jurassic to Early Cretaceous||||||
20834|Yappar Member|41064|6|Mentioned|Fig.5|||||||||
20834|Yappar Member|41361|6|Mentioned|Fig.3|||||||||
20834|Yappar Member|42061|4|Described|p153|||See also Fig.4||||||
20834|Yappar Member|42369|6|Mentioned|p57|||||||||
20834|Yappar Member|42691|5|Briefly described|map legend|Mesozoic||||||||
20834|Yappar Member|42933|5|Briefly described|p236|||of Gilbert River Formation||||||
20834|Yappar Member|43060|5|Briefly described|p58,Table 1c|||of Gilbert River Formation||||||
20834|Yappar Member|43110|5|Briefly described|p54|||of Gilbert River Formation||||||
20834|Yappar Member|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|of Gilbert River Formation||||||
20834|Yappar Member|43287|5|Briefly described|Map Legend||Mesozoic|of Gilbert River Formation. Late Jurassic? to Early Cretaceous.||||||
20834|Yappar Member|43603|5|Briefly described|p9|||||||||
20834|Yappar Member|43625|6|Mentioned|p48|||||||||
20834|Yappar Member|43630|6|Mentioned|Fig.4,p7|||||||||
20834|Yappar Member|43740|6|Mentioned|Fig.5,p45|||||||||
20834|Yappar Member|44246|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
20834|Yappar Member|44926|5|Briefly described|Map Legend|||Late Jurassic? - Early Cretaceous||||||
20834|Yappar Member|45145|3|Fully described|Table 5|||||||||
20834|Yappar Member|50198|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.||||||
20834|Yappar Member|50199|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation.||||||
20834|Yappar Member|50210|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Of the Gilbert River Formation. Overlies: Loth Formation.  Underlies: Coffin Hill Member.||||||
20834|Yappar Member|50595|5|Briefly described|Map Legend|Early Cretaceous|Middle Jurassic|Of the Gilbert River Formation. Underlies: Coffin Hill Member. Overlies: Loth Formation.||||||08-JUL-15
20834|Yappar Member|50627|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|Of the Gilbert River Formation (Eulo Queen Group). Coarse to fine, commonly clayey quartz sandstone and minor lithic quartz sandstone, commonly ferruginised. Overlain by Coffin Hill Member of same formation; overlies Loth Formation.||||||08-JUL-15
20834|Yappar Member|60081|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation. Quartzose sandstone, minor conglomerate.||||||08-JUL-15
20834|Yappar Member|60087|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation. Quartzose sandstone, minor conglomerate,  shale, siltstone.||||||08-JUL-15
20834|Yappar Member|60357|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Of the Gilbert River Formation. Underlies: Coffin Hill Member. Geological Province: Carpentaria Basin.||||||20-AUG-04
20834|Yappar Member|62837|5|Briefly described|Stratigraphic columns|Valanginian|Tithonian|Of the Gilbert River Formation. Age: ~141-~129Ma. Geological Province: Burketown Depression.||||||01-MAR-10
20834|Yappar Member|67402|6|Mentioned|p180|||||Gilbert River Formation||||
20834|Yappar Member|68345|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Unit in Gilbert River Formation.||Is overlain conformably by Coffin Hill Member.|Clayey quartzose sandstone and siltstone, minor mudstone.|
20834|Yappar Member|68349|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Unit in Gilbert River Formation.||Conformably overlies Loth Formation (Eulo Queen Group). Is overlain conformably by Coffin Hill Member.|Clayey quartzose sandstone and siltstone, minor mudstone.|
20834|Yappar Member|68356|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Lower unit in Gilbert River Formation.||Is overlain conformably by Coffin Hill Member.|Clayey quartzose sandstone and siltstone, minor mudstone.|
20834|Yappar Member|68405|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria and Karumba Basins.||Of Gilbert River Formation.||Overlain by Coffin Hill Member.||24-AUG-15
20834|Yappar Member|68417|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|Carpentaria Basin.||Of the Gilbert River Formation.||Conformably overlain by the Coffin Hill Member. Conformably underlain by the Loth Formation.|Clayey quartzose sandstone and siltstone, minor mudstone.|
20834|Yappar Member|69594|5|Briefly described|p521, p540|Early Cretaceous|Late Jurassic|Carpentaria Basin. Fluvial to marine deposition.||Gilbert River Formation.||Is overlain by Coffin Hill Member. Is equivalent to the lower Gilbert River Formation.||
20834|Yappar Member|73147|5|Briefly described|p127, 129-130, 138-140, 144|Early Cretaceous|Early Cretaceous|Smart et al. (1971). Gregory Range area. Age spectra summary diagrams. Also appears as Yapper Member on p144.|130.8 +/- 3.9 Ma (MDA: U-Pb detrital zircon).|Gilbert River Formation.||Conformably overlies Loth Formation (Eulo Queen Group).|Medium-grained quartzose sandstone with conglomeratic bands, current ripple cross-lamination and cross-stratification.|
20835|Yappo Member|24419|5|Briefly described|p16|Proterozoic|Proterozoic|Of Mount Guide Quartzite (lower section). Mainly greywacke-type metasediments, including conglomerate.||||||
20835|Yappo Member|37413|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20835|Yappo Member|37816|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20835|Yappo Member|37862|4|Described|p583|||||||||
20835|Yappo Member|38310|6|Mentioned|p237|||||||||
20835|Yappo Member|38350|4|Described|p9|||||||||
20835|Yappo Member|38442|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mount Guide Quartzite.||||||25-AUG-04
20835|Yappo Member|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20835|Yappo Member|39799|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|Carpentarian||||||
20835|Yappo Member|40623|5|Briefly described|p97|||||||||
20835|Yappo Member|41298|6|Mentioned|Map legend|Carpentarian||||||||
20835|Yappo Member|45161|5|Briefly described|p23|||See also Table 6.||||||
20835|Yappo Member|45166|5|Briefly described|p14|||||||||
20835|Yappo Member|46962|4|Described|Table 1|||||||||
20835|Yappo Member|46995|6|Mentioned|p267|||||||||
20835|Yappo Member|46996|6|Mentioned|p273|||||||||
20835|Yappo Member|49009|2|Defined|p51|Precambrian|Precambrian|Member of Mount Guide Quartzite. See also p7.||||||20-DEC-06
20835|Yappo Member|49041|6|Mentioned|Table 4|||||||||
20835|Yappo Member|50100|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Mount Guide Quartzite.  Mainly greywacke-type metasediments, including conglomerate in lower section and an upper section of ridge-forming , quartz-rich sandstone metamorphosed to quartzite.||||||
20835|Yappo Member|50332|5|Briefly described|p17|Proterozoic|Proterozoic|Of the Mount Guide Quartzite (lower section). Consists of greywacke-type metasediments including conglomerate, and an unamed upper section of ridge-forming, quartz-rich sandstone metamorphosed to quartzite.||||||07-FEB-11
20835|Yappo Member|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Guide Quartzite (Haslingdon Group).||||||
20835|Yappo Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map., p13|Paleoproterozoic|Paleoproterozoic|Leichhardt Superbasin.||Mount Guide Quartzite, Lower Haslingden Group.|||Pebbly greywacke to conglomerate, minor quartzite, feldspathic sandstone and metabasalt; mainly schistose.|
20835|Yappo Member|69591|6|Mentioned|p33|||Mount Oxide and Leichhardt River Domains, Leichhardt Superbasin.||||||
20835|Yappo Member|72684|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Shown as the oldest part of the Haslingden Group. Informally subdivided.||Mount Guide Quartzite||Shown as younger than Bottletree Formation.|Pebbly greywacke to conglomerate, minor quartzite, feldspathic sandstone and metabasalt; mainly sc histose with conglomerate, greywacke, quartzite and feldspathic sandstone.|
20835|Yappo Member|72685|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Leichhardt River Domain. Shown as the oldest part of the Haslingden Group. Informally subdivided.||Mount Guide Quartzite||Shown as younger than Bottletree Formation.|Pebbly greywacke to conglomerate, minor quartzite, feldspathic sandstone and metabasalt; mainly schistose.  Conglomerate, greywacke, quartzite and feldspathic sandstone.|
20852|Yaringa Metamorphics|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Fold Belt.||||||07-NOV-08
20852|Yaringa Metamorphics|24419|5|Briefly described|p14, p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Quartz-mica schist and gneiss, quartzite, migmatite and felsic metaporphyry.  No outcrop on URANDANGI 1:250K sheet.  Unconformably overlain by McNamara Group. Geol. Prov: Western Fold Belt, Leichardt River Subprovince.  See also p15 Fig. 6.||||||07-NOV-08
20852|Yaringa Metamorphics|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20852|Yaringa Metamorphics|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
20852|Yaringa Metamorphics|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|32660|5|Briefly described|Table 5|||||||||
20852|Yaringa Metamorphics|32959|6|Mentioned|p31|||||||||
20852|Yaringa Metamorphics|33214|6|Mentioned|p1279|||||||||
20852|Yaringa Metamorphics|33893|5|Briefly described|p27|||Archaean.||||||
20852|Yaringa Metamorphics|33897|6|Mentioned|p1280|||||||||
20852|Yaringa Metamorphics|33900|6|Mentioned|p7|||Re dates||||||
20852|Yaringa Metamorphics|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|35074|6|Mentioned|Fig.2|||||||||
20852|Yaringa Metamorphics|35139|6|Mentioned|p9|||||||||
20852|Yaringa Metamorphics|35167|6|Mentioned|p151|||||||||
20852|Yaringa Metamorphics|37462|4|Described|Table4.VII|||Also briefly described p266.||||||20-DEC-06
20852|Yaringa Metamorphics|37568|5|Briefly described|p81|||||||||
20852|Yaringa Metamorphics|37862|6|Mentioned|p586|||||||||
20852|Yaringa Metamorphics|38232|6|Mentioned|p83|||||||||
20852|Yaringa Metamorphics|38234|6|Mentioned|p103|||||||||
20852|Yaringa Metamorphics|38584|6|Mentioned|p4|||||||||
20852|Yaringa Metamorphics|39445|5|Briefly described|Table 2|||Minimum age of zircons 2000 Ma. See also p40.||||||20-DEC-06
20852|Yaringa Metamorphics|40840|6|Mentioned|Map legend|||||||||
20852|Yaringa Metamorphics|41298|6|Mentioned|Map legend|Proterozoic||||||||
20852|Yaringa Metamorphics|41381|6|Mentioned|p325|||||||||
20852|Yaringa Metamorphics|41465|5|Briefly described|p6|||||||||
20852|Yaringa Metamorphics|41466|4|Described|p24|||||||||
20852|Yaringa Metamorphics|41721|6|Mentioned|p4|||Geological province: Mt Isa Block.  Lithologically resembles Murphy Metamorphics (Murphy Inlier) and Burrell Creek Formation (Pine Creek Geosyncline).||||||13-MAR-18
20852|Yaringa Metamorphics|41978|6|Mentioned|p497|||||||||
20852|Yaringa Metamorphics|41979|6|Mentioned|p538|||||||||
20852|Yaringa Metamorphics|42367|5|Briefly described|p17|||Age about 1900 Ma U-Pb. Defined by Carter 1961||||||
20852|Yaringa Metamorphics|42565|5|Briefly described|Table 1 P6, P2|||||||||
20852|Yaringa Metamorphics|42706|5|Briefly described|map legend|Proterozoic|Proterozoic|Schist, gneiss, migmatite.   Age is pre-1890-1870Ma Barramundi Orogeny.||||||09-FEB-09
20852|Yaringa Metamorphics|43595|5|Briefly described|p353||Paleoproterozoic|Dated (U-Pb) at 1885+/-10 Ma||||||07-NOV-08
20852|Yaringa Metamorphics|43608|6|Mentioned|Fig.11,p11|||||||||
20852|Yaringa Metamorphics|43928|6|Mentioned|24|||||||||
20852|Yaringa Metamorphics|44195|6|Mentioned|p358||Paleoproterozoic|basement.||||||07-NOV-08
20852|Yaringa Metamorphics|44210|2|Defined|map,Tb.1,p8-10|||||||||
20852|Yaringa Metamorphics|44271|2|Defined|p26,38,45||Archean|||||||07-NOV-08
20852|Yaringa Metamorphics|44275|14|Not recorded|Map Legend|||||||||
20852|Yaringa Metamorphics|44290|2|Defined|p437|||Precambrian possibly Archaean.||||||
20852|Yaringa Metamorphics|44521|14|Not recorded|p8|||||||||
20852|Yaringa Metamorphics|44919|14|Not recorded|p596,(table)||Paleoproterozoic|||||||07-NOV-08
20852|Yaringa Metamorphics|44989|2|Defined|p.58-9|||Tb.III. On many pages. Intruded by Sybella Granite. (F54-1).||||||
20852|Yaringa Metamorphics|45161|6|Mentioned|p9|||||||||
20852|Yaringa Metamorphics|45166|4|Described|p8|||||||||
20852|Yaringa Metamorphics|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
20852|Yaringa Metamorphics|46919|6|Mentioned|p219|||||||||
20852|Yaringa Metamorphics|48997|6|Mentioned|Fig.1|||||||||
20852|Yaringa Metamorphics|49041|5|Briefly described|Table 1|||||||||
20852|Yaringa Metamorphics|50100|6|Mentioned|p26|||Age: >1870Ma.||||||
20852|Yaringa Metamorphics|50332|6|Mentioned|p25|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
20852|Yaringa Metamorphics|50536|5|Briefly described|p11.2|Paleoproterozoic|Paleoproterozoic|Age: ~1890 +/- 8Ma. Intruded by Little Toby Granite.||||||07-NOV-08
20852|Yaringa Metamorphics|60513|6|Mentioned|p281, 282, 283,  p290, p287, 288, 289||||SHRIMP age  1.98 Ga.|||||
20852|Yaringa Metamorphics|61922|5|Briefly described|p19 Fig. 11|||See also p21 Fig.13.||||||
20852|Yaringa Metamorphics|61929|5|Briefly described|p128 Fig. 2|Paleoproterozoic|Paleoproterozoic|Age: 1890+/-8Ma.||||||07-NOV-08
20852|Yaringa Metamorphics|61933|5|Briefly described|p169 Fig.1, p181|||Metamorphosed to upper amphibolite grade between ca 1900 and 1870 Ma.||||||28-APR-06
20852|Yaringa Metamorphics|61936|6|Mentioned|p193|||Includes greenschist facies schist and phyllite||||||
20852|Yaringa Metamorphics|63593|6|Mentioned|p288 Fig.2. |||Western Fold Belt basement. Mis-spelt as Metamorphycs.|||||Schist, gneiss, migmatite.|
20852|Yaringa Metamorphics|63866|4|Described|p57-p58, p64|Orosirian|Orosirian|Leichhardt River Fault Trough. Ages are derived from Page and Williams 1988 and are U-Pb zircon TIMS analyses. A more recent U-PB zircon SHRIMP result of c. 1858 has been interpreted by Bierlein et al (in press).|1900 +/- 14 Ma and 1885 +/- 10 Ma|||Intruded by the Monoghans Granite.|Gneisses.|
20852|Yaringa Metamorphics|64250|6|Mentioned|p8, p9 fig 1, p11 fig 3, p19 |||A basement unit of Western Fold Belt, Mt Isa Inlier. Metamorphosed at 1890 +/- 8 Ma (Page and Williams 1998); crystallisation of igneous phases occurred ca. 1860 - 1850 Ma (Bierlein et al. 2008).|1890 +/- 8 - 1853 +/- 5 Ma|||||
20852|Yaringa Metamorphics|64254|5|Briefly described|p160 Fig. 1, p161, p162, p165, p169|Paleoproterozoic|Paleoproterozoic|Age: ca. 2200Ma (SHRIMP), 2380-2820Ma (Nd model). Geological Province: Kalkadoon - Leichhardt Belt.||||||
20852|Yaringa Metamorphics|64567|5|Briefly described|p1098||Paleoproterozoic|Actually spelt Yaringa metamorphics. About 45 km west of Black Angel Gneiss Complex, but different terranes, not juxtaposed until Mesoproterozoic.||||||21-APR-09
20852|Yaringa Metamorphics|65396|5|Briefly described|p7, p82, p84, p90, p171-172, p175, p186|Orosirian|Orosirian|See also p241, p437-438. Lawn Hill Platform. Basement to Mount Isa Inlier. Metamorphosed at 1890 +/- 8 Ma (Page and Williams, 1988). Crystallisation age c.1853 Ma suggests migmatisation.|1853 +/- 5 Ma (Bierlein and Black, 2005).|||||
20852|Yaringa Metamorphics|67323|5|Briefly described|p6-8, p23, p29, p39, p107|Paleoproterozoic|Paleoproterozoic|See also GIS attrib tbl, Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Pre-Barramundi basement to Ardmore - May Downs, Mount Oxide Domains, Mount Isa Inlier. Protoliths of this unit were metamorphosed during the ~1870-1850 Ma Barramundi Orogeny. Age of metamorphism ~1885 - 1900 Ma.|1890 +/- 8 Ma.|||Intruded by Big Toby, Little Toby and Moonaghans Granites|Quartz - muscovite and quartz - sericite schist and phyllite, quartz - muscovite - biotite gneiss, minor migmatite|
20852|Yaringa Metamorphics|67497|6|Mentioned|p910, p911 Fig.20|Orosirian|Orosirian|Include detrital zircon cores as old as 2200 Ma (Page and Williams 1988).||||||
20852|Yaringa Metamorphics|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province. Pre-Barramundi Orogeny basement. This unit, as well as Saint Ronans Metamorphics and Sulieman Gneiss, are all mapped under the symbol, -Px.||||||
20852|Yaringa Metamorphics|69222|5|Briefly described|p221, p222 Fig.2, p224 Fig.3|Paleoproterozoic|Paleoproterozoic|Basement to Lawn Hill Platform. Metamorphosed during the 1890-1840 Ma Barramundi Orogeny.|1890 +/- 8 Ma|||||09-FEB-18
20852|Yaringa Metamorphics|69591|5|Briefly described|p29-32, p58|Paleoproterozoic|Paleoproterozoic|One of the earliest known successions exposed within the Mount Isa Province: pre-Barramundi Orogeny (>1870 Ma). Considered part of the same depositional package as the Murphy and Yaringa Metamorphics. TIMS ages by Page and Williams (1988). Bierlein et al. (2008) date it at 1874 +/- 3 Ma. Intruded by ~1874 Ma granitoids.|1900 +/- 14 Ma and 1885 +/- 10 Ma.|||Is intruded by Monaghans, Big Toby, and Little Toby Granites.|Quartz-muscovite and quartz-sericite schist and phyllite, quartz-muscovite-biotite gneiss, minor migmatite.|
20852|Yaringa Metamorphics|69917|6|Mentioned|p140|||Western Mount Isa Inlier. Includes ca 1.86-1.88 Ga orthogneisses. Possible source for some of the Entia Dome metasediments (Entia Metamorphics?).||||||
20852|Yaringa Metamorphics|70282|6|Mentioned|p544 Tb.1|||Basement in the Western fold belt, Mount Isa.|1890-1870 Ma|||||13-FEB-18
20852|Yaringa Metamorphics|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1900+/-14 Ma (metamorphism: U-Pb zircon SHRIMP)||||Paragneiss.|
20852|Yaringa Metamorphics|71606|5|Briefly described|p137|Orosirian|Orosirian|Leichardt River Fault Trough, Mount Isa Inlier.||||Overlain by Leichardt Volcanics. Equivalent to Murphy Metamorphics.||
20852|Yaringa Metamorphics|71960|5|Briefly described|p77|Paleoproterozoic||Basement to Mount Isa Group.|>1890 Ma, U-Pb zircon.|||||
20852|Yaringa Metamorphics|72527|6|Mentioned|p184.|Paleoproterozoic|Paleoproterozoic|Mount Isa Orogen. Given as an example of correlated units across the Northern Territory with the Murphy Metamorphics.||||||
20852|Yaringa Metamorphics|72912|5|Briefly described|p12.|Orosirian|Orosirian|Among the oldest known sedimentary rocks exposed in the Mount Isa province.||||||
20852|Yaringa Metamorphics|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
20852|Yaringa Metamorphics|73525|5|Briefly described|p4-5 Fig.2, p19 Fig.13|Orosirian|Orosirian|Leichhardt River Domain.|1890+/-8 Ma metamorphic age||||Metamorphics.|
20863|Yarrabah Granite|39689|6|Mentioned|p65|||||||||
20863|Yarrabah Granite|39997|6|Mentioned|p165|||||||||
20863|Yarrabah Granite|42810|6|Mentioned|p25|||refers to Richards (1977)||||||
20865|Yarrabee Tuff Bed|22990|6|Mentioned|p316|||||||||
20865|Yarrabee Tuff Bed|23007|6|Mentioned|p454|||||||||
20865|Yarrabee Tuff Bed|24093|5|Briefly described|p176 Fig. 2|Permian|Permian|Of the Blackwater Group.  Age: >251Ma.  Geological Province: Bowen Basin.||||||
20865|Yarrabee Tuff Bed|42255|2|Defined|p233|Late Permian||Reserved as Yarrabee Tuff Member.||||||06-OCT-17
20865|Yarrabee Tuff Bed|42932|2|Defined|p67||Late Permian|of Blackwater Group||||||
20865|Yarrabee Tuff Bed|75060|6|Mentioned|p57|||Bowen Basin.|254-252 Ma (Ayaz et al., 2016).|||||
20918|Yates Supersuite|12575|6|Mentioned|p781. |Permian|Permian|I-type granite. Northeastern Hodgkinson Province.|||Includes Puckley Granite.|||
20918|Yates Supersuite|23422|5|Briefly described|Plate 7.3|Late Permian|Late Permian|||||||
20918|Yates Supersuite|23423|4|Described|p312 Table 7.4|Late Permian|Early Permian|I-type granite. Intrudes Hodgkinson Formation. Also see p252. Age: ~280-285 Ma (western group), ~260 Ma (eastern group). Hodgkinson Province.||||||
20918|Yates Supersuite|23426|6|Mentioned|p402.|||||||||
20918|Yates Supersuite|23430|5|Briefly described|493p|||I-Type rocks. Daintree Subprovince. Kennedy Province.||||||
20918|Yates Supersuite|23511|5|Briefly described|Map Legend||Late Permian|||||||
20918|Yates Supersuite|23512|5|Briefly described|Map Legend||Late Permian|||||||
20918|Yates Supersuite|42658|4|Described|p36|||Not related to Yates Creek Formation - reserved by Withnall.||||||22-APR-09
20918|Yates Supersuite|43070|6|Mentioned|p8|||||||||
20918|Yates Supersuite|43098|5|Briefly described|Back pocket map.|||||||||
20918|Yates Supersuite|43285|5|Briefly described|Map Legend||Early Permian|||||||
20918|Yates Supersuite|43625|14|Not recorded|p58|||||||||
20918|Yates Supersuite|50316|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Kennedy Province.||||||
20918|Yates Supersuite|50387|5|Briefly described|Map legend|Permian|Permian|Geological Province: Kennedy Province.||||||
20918|Yates Supersuite|50587|5|Briefly described|Map Legend|Late Permian|Early Permian|Includes: Hope Vale Granite, Normanby Formation. Geological Province: Kennedy Province.||||||28-JUN-04
20918|Yates Supersuite|50596|5|Briefly described|Map Legend|Early Permian|Early Permian|Includes: Leichhardt Pocket Granite.||||||
20918|Yates Supersuite|50630|5|Briefly described|Map Legend|Late Permian|Late Permian|Includes: Trevethan Granodiorite, Mount Yates Granodiorite, Keating Granodiorite.||||||06-JUL-04
20918|Yates Supersuite|60425|3|Fully described|p54 Tb. 4, p90-91|Late Permian|Early Permian|Contains Yates Suite. I-type. Intruded Hodgkinson Fm. Unconformable below Piebald Basalt (Laura Basin). Age details and lithological details  (p91).||||||07-FEB-11
20918|Yates Supersuite|61527|6|Mentioned|p792-793 Fig.2|||I-type. Includes the Bakers Blue pluton.||||||
20918|Yates Supersuite|63140|6|Mentioned|p581.|||To the NE of Hodgkinson Province.|||||I-type granites.|
20918|Yates Supersuite|66852|5|Briefly described|pp938-939, p941.|||The geometry of its plutons has been influenced by the  WNW-ESE Desailly Structure, described in the article. One pluton is truncated by a WNW-ESE fault.||||||
20918|Yates Supersuite|68553|6|Mentioned|Map legend|Permian|Permian|This unit is mapped, under the symbol Pgk, with the following: Cape Melville, Kangaroo Creek, Cooktown, Lags, Pieter Botte, Weymouth, Whypalla, Woodstock and Brodies Camp Supersuites; parts of Almaden, Leichhardt and O'Briens Creek Supersuites; Mount Alto, Tinaroo and Wangetti Suites; and various ungrouped Permian plutonic units.||||||
20918|Yates Supersuite|69030|5|Briefly described|p6|Permian|Permian|Palmer-Barron Subprovince, Hodgkinson Province.|286 +/- 4 Ma (SHRIMP).||||I-type granitoids.|
20918|Yates Supersuite|69593|4|Described|p478, p480, p482-483, p511|Permian|Permian|Daintree Subprovince, Kennedy Igneous Association. Crops out over ~134 km2. A western group is associated with Whypalla Supersuite; an eastern group with Cooktown Supersuite.|~280 Ma (in the west) to ~260 Ma (in the east).||Bakers Blue, Leichhardt Pocket, Puckley, Hope Vale, Black Mountain Granites; Howick Island, Keating, Mount Yates, Talgijah, Trevethan Granodiorites.||I-type. More mafic than other I-type granitoids in the Subprovince. Even-grained to highly porphyritic, hornblende-biotite and (hornblende-) biotite granodiorite and granite; rare orthopyroxene and clinopyroxene.|
20918|Yates Supersuite|72983|6|Mentioned|p3, p35, p38||||||Hope Vale Granite, Puckley Granite||I-type igneous rocks.|
20921|Yatton Limestone|23042|4|Described|p51,7||Permian|Of Apis Creek Formation.[?]||||||02-NOV-05
20921|Yatton Limestone|32943|6|Mentioned|p106|||||||||
20921|Yatton Limestone|32945|6|Mentioned|p88|||Permian||||||
20921|Yatton Limestone|36739|6|Mentioned|p17|||||||||
20921|Yatton Limestone|43987|14|Not recorded|p267|||See also Lexicon.||||||
20921|Yatton Limestone|44311|14|Not recorded|p202|||||||||
20921|Yatton Limestone|44347|14|Not recorded|p76|||North of Clermont. See also Lexicon.||||||
20921|Yatton Limestone|44725|14|Not recorded|p203|||Basal member of Apis Creek Formation.||||||
20921|Yatton Limestone|44858|14|Not recorded|p94|||||||||
20921|Yatton Limestone|45071|6|Mentioned|p69|||||||||
20921|Yatton Limestone|48898|6|Mentioned|p33|||||||||
20921|Yatton Limestone|60480|5|Briefly described|Map Legend|Early Permian|Early Permian|Of the Back Creek Group. Fossiliferous limestone, calcareous siltstone, mudstone, siltstone, lithic sandstone.||||||
20921|Yatton Limestone|61035|5|Briefly described|p15|||Basal part of the Back Creek Group, on the western flank. Maximum thickness: 30m||||||07-FEB-11
20921|Yatton Limestone|65388|5|Briefly described|p142, 175, 179 Fig.68|Permian|Permian|Of lowermost Back Creek Group. Previously included in Apis Creek Formation, but now considered a Formation-level unit in Back Creek Group. Fossiliferous.||||||
20921|Yatton Limestone|68679|5|Briefly described|p378, p380|||Withnall et al. (2009). Bowen Basin. 40m thick. Shallow-marine shelf sediments.||||Correlated (probably) with Tiverton Formation.|Limestone (bioclastic, brachiopodal calcarenite and coquinite).|
20928|Yeldham Granite|22438|4|Described|p545-547, Fig.12||Paleoproterozoic|Age of unit 1820 Ma||||||07-NOV-08
20928|Yeldham Granite|22457|6|Mentioned|Fig31 P32, Fig29|||||||||
20928|Yeldham Granite|22680|6|Mentioned|85|||||||||
20928|Yeldham Granite|23198|6|Mentioned|p873, 876|||||||||
20928|Yeldham Granite|23393|4|Described|p18, p16 Fig. 4|Paleoproterozoic|Paleoproterozoic|Intrudes the Kamarga Volcanics.  Age: ~1820Ma.  Geological Province: Lawn Hill Sub-province.||||||07-NOV-08
20928|Yeldham Granite|23406|5|Briefly described|p601 Fig.3|||||||||
20928|Yeldham Granite|23408|6|Mentioned|p515, p516 Fig. 5|||Onlapped by Torpedo Creek Quartzite.  Includes igneous rocks.||||||15-JUN-09
20928|Yeldham Granite|23409|5|Briefly described|p535 Fig.2|||||||||
20928|Yeldham Granite|23545|5|Briefly described|Fig 1 p604|||||||||
20928|Yeldham Granite|23767|5|Briefly described|p1954 Fig. 1a|||Geological Province: Mount Isa Superbasin.||||||20-DEC-06
20928|Yeldham Granite|23958|5|Briefly described|p1133|||||||||
20928|Yeldham Granite|24197|5|Briefly described|p96 Tb. 12.1|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province:Mount Isa Inlier. Table numbered incorrectly as Tb. 1.1.||||||07-FEB-11
20928|Yeldham Granite|24309|5|Briefly described|p1017|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20928|Yeldham Granite|24419|6|Mentioned| p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: Western Fold Belt, Lawn Hill Subprovince (Mount Isa Orogen).||||||07-NOV-08
20928|Yeldham Granite|24432|6|Mentioned|p565 Fig.4|||||||||
20928|Yeldham Granite|36548|2|Defined|p517|Precambrian|Precambrian|||||||
20928|Yeldham Granite|37459|6|Mentioned|p423|||||||||
20928|Yeldham Granite|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20928|Yeldham Granite|38310|6|Mentioned|p237|||||||||
20928|Yeldham Granite|38348|4|Described|p5|||||||||
20928|Yeldham Granite|38900|6|Mentioned|p62|||||||||
20928|Yeldham Granite|39445|5|Briefly described|Table 2|||See also p40.||||||20-DEC-06
20928|Yeldham Granite|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
20928|Yeldham Granite|39925|6|Mentioned|p334|||See also Fig.9.||||||
20928|Yeldham Granite|39943|6|Mentioned|Table 1A|||||||||
20928|Yeldham Granite|39944|3|Fully described|p229|||||||||
20928|Yeldham Granite|40840|6|Mentioned|Map legend|||||||||
20928|Yeldham Granite|41465|6|Mentioned|p8|||||||||
20928|Yeldham Granite|41979|4|Described|p517|||||||||
20928|Yeldham Granite|42565|5|Briefly described|Table 2 P7|||||||||
20928|Yeldham Granite|45166|5|Briefly described|p17|||||||||
20928|Yeldham Granite|47083|5|Briefly described|p20|||Previously mapped as part of the Weberra Granite.||||||
20928|Yeldham Granite|49041|5|Briefly described|Table 1|||Mention Table 4.||||||20-DEC-06
20928|Yeldham Granite|50536|5|Briefly described|p1.5, 11.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Mount Isa Inlier. Of the Yeldham Suite. Age: ~1820Ma. Overlain by  McNamara Group.||||||07-NOV-08
20928|Yeldham Granite|50624|5|Briefly described|p234 Fig.2||Paleoproterozoic|||||||07-NOV-08
20928|Yeldham Granite|61929|5|Briefly described|p128 Fig. 2|||||||||
20928|Yeldham Granite|61936|6|Mentioned|p193|Paleoproterozoic|Paleoproterozoic|Age: ~1820Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier.||||||07-NOV-08
20928|Yeldham Granite|63109|6|Mentioned|p1109|||Low density granite.||||||30-SEP-08
20928|Yeldham Granite|63866|5|Briefly described|p57|Statherian|Statherian|Lawn Hill Platform, Leichhardt Superbasin. Crops out in the Kamarga Dome. A zircon U-Pb TIMS age of c. 1820 Ma is derived from Wyborn et al., 1988.|1796 +/- 3 Ma (xenotime TIMS)|||Intrudes the Kamarga Volcanics.||
20928|Yeldham Granite|64250|6|Mentioned|p17 fig 7, p11 fig 3, p21|||Western Fold Belt, Mount Isa Inlier. Preceded the accumulation of the Leichhardt Superbasin (c.1800-1750 Ma).|~1820 Ma|||||
20928|Yeldham Granite|64575|6|Mentioned|p656|||Age: 1820Ma.||||||
20928|Yeldham Granite|65337|6|Mentioned|p6 Fig.3.|||||||||
20928|Yeldham Granite|65396|5|Briefly described|p82, p175, p192, p195, p241|Orosirian|Orosirian|Lawn Hill Platform. Its emplacement preceded the accumulation of the Leichhardt Superbasin. Formations with detrital zircons from this unit are listed.|1820 Ma|||||
20928|Yeldham Granite|67323|5|Briefly described|GIS attrib tbl, p6, p10, p23, p30, p107|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map, Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Century Domain, Mount Isa Inlier. Lawn Hill region. Post-Barramundi Orogeny. Intrusions 1820-1800 Ma.Yeldham Igneous Event (intraplate magmatism). TIMS xenotime age ~1793 Ma. 1796+/-3 Ma (Wyborn et al 1988, Neumann & Fraser, 2007). U-Pb TIMS age ~1820 Ma (2001).|1796 +/- 3 Ma.|||intrudes Kamarga Volcanics. Age correlation with Big Toby and Monaghans Granites. Underlies McNamara Group.|Medium-grained muscovite leucogranite; pegmatite dykes and minor greisen|
20928|Yeldham Granite|68542|6|Mentioned|p1 |||||||||
20928|Yeldham Granite|68553|6|Mentioned|Map legend; schematic diagram.|Paleoproterozoic|Paleoproterozoic|Mount Isa Province.||||||
20928|Yeldham Granite|68576|6|Mentioned|Q_2: p1|Paleoproterozoic|Paleoproterozoic|Mount Isa area.||||||
20928|Yeldham Granite|69222|6|Mentioned|p222 Fig.2|||Associated with 1890-1840 Ma Barramundi Orogeny.||||||
20928|Yeldham Granite|69591|5|Briefly described|p28, p30, p32, p40, p42, p60, p105|Paleoproterozoic|Paleoproterozoic|Century Domain, Mount Isa Province. An age of ~1790 Ma (Hutton, 1983) is also given.|1796 +/- 3 Ma (Wyborn et al., 1988).|||Intrudes Kamarga Volcanics. Is overlain nonconformably by Torpedo Creek Quartzite (Gun Supersequence).|Medium-grained muscovite leucogranite; pegmatite dykes and minor greisen.|
20928|Yeldham Granite|71592|5|Briefly described|Appendix A.|||Century Domain, Mount Isa Orogen.|1796+/-3 Ma (crystallisation: xenotime U-Pb TIMS).||||Granite.|
20928|Yeldham Granite|72526|5|Briefly described|p6 Fig.1.2,|Paleoproterozoic|Paleoproterozoic|Shown with South Nicholson Granite Complex.||||||
20928|Yeldham Granite|72889|6|Mentioned|p6 Fig.i.|||||||||
20928|Yeldham Granite|73413|6|Mentioned|p3|||Mount Isa Inlier, Western Fold Belt, Lawn Hill Platform.||||||
20928|Yeldham Granite|73553|6|Mentioned|p259|Statherian|Statherian|Kamarga Dome.|1796+/-3 Ma (Wyborn et al., 1988)|||||
20938|Yellow Jacket Rhyolite|23291|4|Described|p95 Tb. 3.10|Carboniferous|Carboniferous|Parent: Eveleigh Volcanic Subgroup. Thickness: ~560m. Geological Province: Georgetown Region.||||||28-MAY-15
20938|Yellow Jacket Rhyolite|23513|5|Briefly described|Map legend||Carboniferous|Palaeozoic Volcanic No. V28. I-Type.||||||
20938|Yellow Jacket Rhyolite|23619|4|Described|p32 Table 1||Carboniferous|Intruded by Caterpillar Microgranite. Eveleigh Volcanic Subgroup, of Newcastle Range Volcanic Group. Beril Peak Rhyolite, Gilberton Formation.||||||
20938|Yellow Jacket Rhyolite|39917|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
20938|Yellow Jacket Rhyolite|43113|4|Described|Table 1 p19||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
20938|Yellow Jacket Rhyolite|43253|5|Briefly described|map legend||Carboniferous|of Eveleigh Volcanic Subgroup||||||
20938|Yellow Jacket Rhyolite|43259|4|Described|Appendix 1,p3.||Carboniferous|of Eveleigh Volcanic Subgroup.||||||
20938|Yellow Jacket Rhyolite|43740|4|Described|p12|||||||||
20938|Yellow Jacket Rhyolite|50198|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Of the Eveleigh Volcanic Subgroup (Of the Newcastle Range Volcanic Group).||||||
20938|Yellow Jacket Rhyolite|60360|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Rhyolitic ignimbrite, basalt, andesite, sandstone, siltstone and conglomerate. Of the Eveleigh Volcanic Subgroup.||||||19-AUG-04
20938|Yellow Jacket Rhyolite|68354|5|Briefly described|Map legend.|Early Carboniferous|Early Carboniferous|Kennedy Province.||Unit in Eveleigh Volcanic Subgroup.|Includes Pint Pot Andesite Member.||Rhyolitic ignimbrite with locally abundant lithic clasts; minor hornblende-pyroxene andesite and basaltic andesite; rhyolitic volcanic lutite to crystal- and lithic-rich volcanic arenite and lutite.|
20938|Yellow Jacket Rhyolite|68477|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Kennedy Province. The 3 facies are mapped separately.||Of the Eveleigh Volcanic Subgroup.|||Rhyolitic ignimbrite with abundant lithic clasts, minor hornblende-pyroxene andesite and basaltic andesite, rhyolitic volcanic lutite to arenite and rudite; aphyric basalt and/or andesite; volcaniclastic sandstone, siltstone and conglomerate.|
20945|Yelvertoft Bed|22954|6|Mentioned|Fig3p9|Middle Cambrian|Early Cambrian|||||||
20945|Yelvertoft Bed|30479|6|Mentioned|Fig.7|||Stratigraphic relationships||||||
20945|Yelvertoft Bed|30778|6|Mentioned|p5,Fig.5|||||||||
20945|Yelvertoft Bed|31289|6|Mentioned|p704|||||||||
20945|Yelvertoft Bed|33111|6|Mentioned|Fig.16|||||||||
20945|Yelvertoft Bed|34287|6|Mentioned|Fig.3|||||||||
20945|Yelvertoft Bed|37572|4|Described|p157|||See also Fig.7||||||
20945|Yelvertoft Bed|40996|6|Mentioned|p403|||||||||
20945|Yelvertoft Bed|44091|14|Not recorded|p16,Tb.1,18||Middle Cambrian|||||||
20945|Yelvertoft Bed|45044|14|Not recorded|p1,3,4,20-26,28,30-1||Middle Cambrian|||||||
20945|Yelvertoft Bed|45052|6|Mentioned|p90|||M.Camb. Beetle Ck. Fm.||||||
20945|Yelvertoft Bed|45055|6|Mentioned|p6|||Cambrian. Fossil locality P7.||||||22-FEB-16
20945|Yelvertoft Bed|47058|6|Mentioned|Fig.9 P131|||||||||
20945|Yelvertoft Bed|48971|6|Mentioned|p10|||See also P14, P15, P18, P21, P24, P27.||||||
20945|Yelvertoft Bed|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Contains fauna of Ordian age.||||||
20945|Yelvertoft Bed|64068|5|Briefly described|p57|||David (1932) p29.||Of Thorntonia Limestone.|||Chertified dolostone.|22-FEB-16
20945|Yelvertoft Bed|69443|5|Briefly described|p28:16|Middle Cambrian|Middle Cambrian|David (1932).||Thorntonia Limestone.|||Chertified dolostone.|12-JUL-16
20945|Yelvertoft Bed|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. Occurs as a 5m-thick section at Halls Memorial on the Barkly Highway. Contains the zone trilobite Redlichia chinensis (Opik 1970) and a varied bradoriid fauna.||Beetle Creek Formation.|||Fossiliferous chert.|
21012|Yorkeys Diorite|24382|5|Briefly described|Map legend|Triassic|Permian|||||||
21012|Yorkeys Diorite|41778|2|Defined|Table 3|Triassic|Permian|||||||
21012|Yorkeys Diorite|42054|6|Mentioned|p273|||||||||
21012|Yorkeys Diorite|63821|5|Briefly described|p29|Triassic|Permian|Intrudes sediments of Curtis Island Group. A zoned intrusion with a marginal phase of medium-grained gabbro to diorite, successive inner zones of quartz diorite to granodiorite, and a small central core of granite.||||||07-FEB-11
21012|Yorkeys Diorite|68679|5|Briefly described|p409, p411|Late Triassic|Late Triassic|Northern New England Orogen. Outcrop area ~4 km2.||Station Creek Igneous Complex.|||Hornblende diorite, quartz diorite, granite; zoned, with marginal gabbro to diorite, quartz diorite to granodiorite phases and small granitic core.|
21016|Youlambie Conglomerate|22973|5|Briefly described|p9 Fig.2 (a)|Early Permian|Early Permian|||||||
21016|Youlambie Conglomerate|22977|5|Briefly described|p67 Fig.2|Late Permian|Late Permian|||||||
21016|Youlambie Conglomerate|23037|6|Mentioned|p12,34,6,40,48,57|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|23468|5|Briefly described|Fig 2 p 295|||||||||
21016|Youlambie Conglomerate|24076|5|Briefly described|p397 Fig. 2|Early Permian|Early Permian|Max. thickness: 1830m.  Geological Province: Yarrol Basin.||||||
21016|Youlambie Conglomerate|24488|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|24489|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|24491|5|Briefly described|p14, 19|Early Permian|Namurian|||||||
21016|Youlambie Conglomerate|24615|5|Briefly described|CD|Early Permian|Late Carboniferous|[CPy].  granule to boulder polymictic conglomerate commonly with granite and rhyolite clasts, felsic volcaniclastic sandstone, tuffaceous and carbonaceous siltstone and mudstone, dacitic to rhyolitic ignimbrite, breccia, minor coal.||||||
21016|Youlambie Conglomerate|29728|6|Mentioned|p394|||Molluscan content.||||||
21016|Youlambie Conglomerate|30059|6|Mentioned|p5|||Lower Permian age.||||||
21016|Youlambie Conglomerate|30450|6|Mentioned|p7|||Fauna. Yarrol Basin||||||
21016|Youlambie Conglomerate|30451|4|Described|p37|||Refers Dear (1968). See also P38||||||
21016|Youlambie Conglomerate|30840|6|Mentioned|p780|||||||||
21016|Youlambie Conglomerate|30914|6|Mentioned|Map legend|Permian|Permian|||||||
21016|Youlambie Conglomerate|30916|6|Mentioned|p96|||||||||
21016|Youlambie Conglomerate|31656|4|Described|Table 1|||L.Permian||||||
21016|Youlambie Conglomerate|31657|4|Described|p95|||See also P101. Sakmarian||||||
21016|Youlambie Conglomerate|31658|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
21016|Youlambie Conglomerate|31659|4|Described|p2, p58, p59-60|Early Permian|Early Permian|Age: Lower Permian (Sakmarian). Dominantly terrestrial deposits - conglomerate with granite phenoclasts, lithic and feldspathic. See also Table 1.||||||08-OCT-08
21016|Youlambie Conglomerate|32094|6|Mentioned|p383|||||||||
21016|Youlambie Conglomerate|32141|6|Mentioned|p153|||||||||
21016|Youlambie Conglomerate|32358|4|Described|Table 2|||P15||||||
21016|Youlambie Conglomerate|32496|6|Mentioned|Map legend|Permian|Permian|||||||
21016|Youlambie Conglomerate|32836|6|Mentioned|p5|||||||||
21016|Youlambie Conglomerate|32943|6|Mentioned|p87|||See also P106. Allandale age. fauna||||||
21016|Youlambie Conglomerate|32945|6|Mentioned|p74|||See also P75,87 & Fig.1.||||||
21016|Youlambie Conglomerate|33728|6|Mentioned|p37|||See also P38.||||||
21016|Youlambie Conglomerate|33774|6|Mentioned|p29|||Correlation||||||
21016|Youlambie Conglomerate|34085|6|Mentioned|Cor.chart|||Stephanian||||||
21016|Youlambie Conglomerate|34132|6|Mentioned|p4|||Lower Permian||||||
21016|Youlambie Conglomerate|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
21016|Youlambie Conglomerate|34408|6|Mentioned|p185|||On Table||||||
21016|Youlambie Conglomerate|35069|6|Mentioned|Fig.1|||||||||
21016|Youlambie Conglomerate|36045|6|Mentioned|p329|||See also P330.||||||
21016|Youlambie Conglomerate|36235|6|Mentioned|Fig.1|||||||||
21016|Youlambie Conglomerate|36488|6|Mentioned|Plate 1|||||||||
21016|Youlambie Conglomerate|36825|6|Mentioned|p2|||||||||
21016|Youlambie Conglomerate|37109|6|Mentioned|p283|||||||||
21016|Youlambie Conglomerate|37119|6|Mentioned|Fig.1|||||||||
21016|Youlambie Conglomerate|38081|5|Briefly described|Table 1|||||||||
21016|Youlambie Conglomerate|38153|6|Mentioned|p368|||||||||
21016|Youlambie Conglomerate|38406|6|Mentioned|p11|||||||||
21016|Youlambie Conglomerate|38447|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
21016|Youlambie Conglomerate|39252|5|Briefly described|p16|||||||||
21016|Youlambie Conglomerate|39445|5|Briefly described|Table 7|||See also Table 8||||||
21016|Youlambie Conglomerate|39632|6|Mentioned|p209|||||||||
21016|Youlambie Conglomerate|40623|5|Briefly described|p79|||||||||
21016|Youlambie Conglomerate|41246|6|Mentioned|Map legend|Permian||||||||
21016|Youlambie Conglomerate|41576|6|Mentioned|p17|||||||||
21016|Youlambie Conglomerate|41922|4|Described|Table 1, P10|||||||||
21016|Youlambie Conglomerate|42547|4|Described|p50, 51, 53|||||||||
21016|Youlambie Conglomerate|42980|5|Briefly described|p307|||||||||
21016|Youlambie Conglomerate|42987|5|Briefly described|p27|||||||||
21016|Youlambie Conglomerate|43017|5|Briefly described|Fig.3,p375|||||||||
21016|Youlambie Conglomerate|43018|6|Mentioned|p388|||||||||
21016|Youlambie Conglomerate|43775|6|Mentioned|p29|||||||||
21016|Youlambie Conglomerate|44337|5|Briefly described|Map Legend||Early Permian|Lithology.||||||
21016|Youlambie Conglomerate|44360|14|Not recorded|p30-32||Early Permian|||||||
21016|Youlambie Conglomerate|44379|2|Defined|p1,2,11,13,16-9,23-5||Sakmarian|Tb.3,map.||||||
21016|Youlambie Conglomerate|44487|14|Not recorded|p201||Permian|||||||
21016|Youlambie Conglomerate|45071|3|Fully described|Table 11|||||||||
21016|Youlambie Conglomerate|45097|6|Mentioned|p23|||Eurydesma. Correlation chart.||||||
21016|Youlambie Conglomerate|48898|4|Described|p18|||See also PP24,82||||||
21016|Youlambie Conglomerate|50190|6|Mentioned|p30, 60|||||||||
21016|Youlambie Conglomerate|50197|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|50208|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|50209|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|50213|5|Briefly described|Map legend|Early Permian|Late Carboniferous|Granule to boulder polymictic conglomerate.  Overlain by Rookwood Volcanics.||||||17-MAY-04
21016|Youlambie Conglomerate|50214|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Overlies Rockhampton Group.||||||17-MAY-04
21016|Youlambie Conglomerate|50215|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Granule to boulder polymictic conglomerate - more lithology included.||||||18-JUN-09
21016|Youlambie Conglomerate|50317|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|50602|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Polymitic conglomerate with abundant granite and rhyolite clasts, felsic volcaniclastic sandstone, tuffaceous and carbonaceous siltstone and mudstone, dacitic to rhyolitic ignimbrite. Underlies: Rookwood Volcanics.||||||19-JUL-04
21016|Youlambie Conglomerate|60282|5|Briefly described|p5, p9|Westphalian|Westphalian|Polymictic, granite and rhyolite-bearing conglomerate, lithofeldspathic to lithic sandstone, laminated siltstone and mudstone, and rhyolitic igmimbrite.  Age: ~305Ma.  Geological Province: Yarrol Province.  See also p45.||||||28-APR-05
21016|Youlambie Conglomerate|60557|5|Briefly described|p19 Fig. 5b, p24|Early Permian|Late Carboniferous|Overlies the Lorray Formation.  See also p20 Fig. 5c.||||||09-JUN-05
21016|Youlambie Conglomerate|61035|6|Mentioned|p12, p13|Permian|Early Permian|||||||07-FEB-11
21016|Youlambie Conglomerate|61612|6|Mentioned|p270 Fig. 1|Early Permian|Late Carboniferous|||||||
21016|Youlambie Conglomerate|61772|6|Mentioned|p128 Fig. 1||Carboniferous|In New England Orogen.||||||23-SEP-08
21016|Youlambie Conglomerate|61777|5|Briefly described|p224, p230, p225 Tab. 1|||Age: 299.3+/-5.5, 301.3+/-3.2, 303.1+/-2.5, 304+/-5.6, 309.5+/-4.7Ma (SHRIMP U/Pb). Combined ages give 303.1+/-2.5Ma. Geological Province: Yarrol Province.||||||07-FEB-11
21016|Youlambie Conglomerate|61782|6|Mentioned|p279, p280, p282|||||||||
21016|Youlambie Conglomerate|61791|6|Mentioned|p326 Fig. 2|Permian|Carboniferous|||||||
21016|Youlambie Conglomerate|63832|5|Briefly described|p131 fig 2, p135|Cisuralian||Jones (2003). Northern New England Fold Belt; east Bowen Basin. Spans fifth (P1) and sixth (P2) glaciations.|||||Includes a thick succession of interbedded diamictites, deformed sandstones and conglomerates, rhythmically laminated mudrocks with outsize gravel.|14-DEC-17
21016|Youlambie Conglomerate|64631|5|Briefly described|p44 Fig.2, p48, 49.|Artinskian|Asselian|Northern New England Fold Belt. Shows evidence of glaciation. Biostratigraphic age control for base and top.||||Is overlain by Yarrol Formation.||
21016|Youlambie Conglomerate|64855|6|Mentioned|p29|Early Permian|Late Carboniferous|||||||22-FEB-10
21016|Youlambie Conglomerate|65388|3|Fully described|p47-50; p48, 49, 19, 20, 28, 31, |Artinskian|Late Carboniferous|Rockhampton Subprovince or Grantleigh Subprovince, Yarrol Province.Named and decribed by Dear (1968). Age of ignimbrites: 303+/-2.5 Ma. Conformably underlies and apparently interfingers with Rookwood Volcanics. Overlies Lorray Formation in places, but ages overlap. Unconformably overlain by Alton Downs Basalt and Mount Salmon Volcanics. Correlated with either Torsdale Volcanics or Bulgi Conglomerate Member (Camboon Volcanics) - fossil leaves.  Also correlated with Carmila beds,  upper Lizzie Creek Volcanic Group. Quail Island rocks are now assigned to Wongrabry beds. Unconformably overlain by Muncon Volcanics. Conglomerate, though not dominant, is characteristic. Includes granite and rhyolite-bearing conglomerate; lithofeldspathic to lithic quartz-bearing sandstone; thinly bedded to laminated siltstone and mudstone, locally carbonaceous; and minor rhyolitic ignimbrite. See also p46, 58, 78, 80, 142, 174, 208, 439, 447.||||||
21016|Youlambie Conglomerate|68008|2|Defined|p2, p17, p48, p64, p67, p70-71, p73, p77|Permian|Late Carboniferous|See also p79-80, p91, p109, p121, p123-134, p147, p156-157, p184, p188, p193-194, p203, p209, p219, p222, p251,  p261, p323, p343-344, p346, p368-369, p372, p375-376, p378, p381, p384, p393, p480-481, p491, p526, p534-541, p569, p581, p583, p590, p626. Dear (1968). Its area was extended during the 1960s. Forms a discontinuous NW-trending belt 250 x 25km. 1320m thick in the type section, two overlapping parts beside Youlambie Creek, 13km N of Monto; modified to produce a generalised stratigraphic section (illustrated). The oldest unit in an extension-related package. Geochemistry described. Extremely low magnetic response. Fluvial, lacustrine and ?glacial deposits. Abundant plant stem and leaf fossils; thin beds with marine fossils; species listed and discussed. Facies and facies associations very well described and illustrated. Overlaps the Lorray Formation in age (discussed). Is overlain conformably by Rookwood Volcanics, Yarrol Formation or Smoky beds, and unconformably by Winterbourne, Mount Salmon, Inverness, Muncon Volcanics, Callide Coal Measures or Dinner Creek Conglomerate. Is faulted against Craigilee and Cynthia beds and Rookwood Volcanics. Intruded by Flaggy Quartz Monzodiorite, Sawnee Gabbro, Dumgree Tonalite, and Bocoolima, Rocky Point, Ridgelands Granodiorites. Probable correlative of Mount Bulgi Conglomerate. Several similar ages given (Fanning, 2012). Geophysics modelling.|300.8 +/- 3.4 Ma (interbedded ignimbrite).|||Conformably overlies Lorray Formation. Unconformably overlies Rockhampton Group, Marble Waterhole beds, Three Moon Conglomerate, Mount Hoopbound, Balaclava and Lochenbar Formations. See Comments.|Characterised by conglomerate with clasts of granite and rhyolite. Also brown lithofeldspathic to lithic quartz-bearing sandstone; grey siltstone and mudstone, locally carbonaceous; varved siltstone; minor rhyolitic ignimbrite.|
21016|Youlambie Conglomerate|68359|6|Mentioned|p9|||||||||
21016|Youlambie Conglomerate|68553|6|Mentioned|Map legend; schematic diagram.|Early Permian|Late Carboniferous|Yarrol Province. This unit, as well as Glenprairie beds and Wongrabry beds, are all mapped under the symbol, CPy.||||||
21016|Youlambie Conglomerate|68679|5|Briefly described|p312-313, p316, p337-338, p344-345, p349|Permian|Late Carboniferous|See also p352, p379, p398, p425, p469. Dear (1968). Crops out in a discontinuous, NW-trending belt 250km long and up to 25km wide, from Monto to Develin homestead. Northern New England Orogen. An extensional unit. Braided stream and proglacial lacustrine (varved shale) deposits with short marine incursions. Abundant Permian plant fossils. RELATED UNITS (continued): Is intruded by the Bocoolima, Rocky Point Granodiorites, Dumgree Tonalite, Sawnee Gabbro (Galloway Plains Igneous Complex), Kyle Mohr Igneous Complex and Craiglands Quartz Monzodiorite.|~300 Ma (Withnall et al., 2009).|||Unconformably overlies Marble Waterhole beds. Is overlain conformably by Rookwood Volcanics. Probably equivalent to the Glenprairie beds. See COMMENTS for list of intruding units.|Thick-bedded, pebble to boulder conglomerate, commonly polymict with rounded granite and rhyolite clasts; commonly interbedded with lithofeldspathic to lithic quartzose sandstone; minor rhyolitic ignimbrite; interbedded mudstone and siltstone.|
21016|Youlambie Conglomerate|70373|6|Mentioned|p801 |Permian|Asselian|Jones (2003). Yarrol Block, northern New England Orogen.||||Correlated with Alum Rock beds.||28-SEP-16
21016|Youlambie Conglomerate|71592|5|Briefly described|Appendix A.||||301+/-3.4 Ma (SHRIMP U-Pb zircon).||||Rhyolite.|
21016|Youlambie Conglomerate|73197|6|Mentioned|p467, p470|Late Carboniferous|Late Carboniferous|New England Orogen, northern. Yarrol Province. Forearc basin, terrestrial environment.||||||
