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
967|Ball Bay Basalt|31571|2|Defined|p247|Pliocene|Pliocene|||||||
967|Ball Bay Basalt|61942|5|Briefly described|p244|Pliocene|Pliocene|Underlies: Steels Point Basalt. Age: 3.01-3.08 +/- 0.06My. Thinly columnar and hackly jointed lava, breccia||||||
74901|Barracouta Shoal Formation|69297|6|Mentioned|p305|Holocene|Messinian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlies the Oliver Formation. ||
74901|Barracouta Shoal Formation|69452|5|Briefly described|p36:15, 22|Holocene|Pliocene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
74901|Barracouta Shoal Formation|69673|6|Mentioned|p174|||||||||
74901|Barracouta Shoal Formation|70061|5|Briefly described|Regional geology Figs.6-7, p12|Holocene|Miocene|See also Sahul: Fig.2. Vulcan: Fig.2. [Misleadingly abbreviated to Barracouta Formation, a Victorian unit, on p12.]||Woodbine Group.||Overlies Oliver Formation.||12-JUL-16
74901|Barracouta Shoal Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Holocene|Miocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Woodbine Group.||Overlies Oliver Formation.||12-JUL-16
1240|Bassett Formation|7142|6|Mentioned|p350 Fig.4.|Paleogene|Late Cretaceous|Browse Basin.||||Overlies Puffin Formation. Is overlain by Prion and Grebe Formations.||
1240|Bassett Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|||||Overlies Puffin Formation. Is overlain by Prion and Grebe Formations.||
1240|Bassett Formation|13354|6|Mentioned|p375 Fig.6.|Palaeogene|Palaeogene|Unit of Woodbine Group. Overlies Puffin Formation of Bathurst Island Group and underlies Grebe and Prion Formations.||116||||28-OCT-14
1240|Bassett Formation|42053|5|Briefly described|Fig.3 p30|||||||||30-APR-12
1240|Bassett Formation|63358|5|Briefly described|p4 Fig. 1.3|Paleocene|Maastrichtian|||||||
1240|Bassett Formation|69297|5|Briefly described|p305|Ypresian|Danian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlies the Puffin Formation. ||
1240|Bassett Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Ypresian|Danian|See also Northern: Fig.2; p1, p3. Yampi: Fig.2. Browse Basin. Oil show in the Phrixus 1 well. Potential intraformational seals.||Woodbine Group.||Overlies Puffin Formation. Equivalent to Johnson Formation.||12-JUL-16
38064|Blue Whale Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Ceduna Formation.||||||
38064|Blue Whale Supersequence|61544|6|Mentioned|p367 Fig.3. |Albian|Albian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.||
38064|Blue Whale Supersequence|66578|6|Mentioned|p1007 Fig.3.|Cretaceous|Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.||
38064|Blue Whale Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Cenomanian|Albian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in marine to deltaic environments during the first marine flooding event of the Ceduna Sub-basin. Good potential oil and gas source rocks with high organic content. Interpreted pre-deformation thickness of 1500-2000m. See also p26 fig 2.11, p41, p43, p44, p45 fig 2.17, p58, p60, p61.||||Overlies the Bronze Whaler Supersequence. Overlain by the White Pointer Supersequence. ||
38064|Blue Whale Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2|Cenomanian|Albian|Bight Basin. Comprises Ceduna Formation and topmost Upper Borda Formation. Marine shales are potential source rocks and form a regional seal.||||Overlies Bronze Whaler Supersequence. Is overlain by White Pointer Supersequence.|Marine silts and shales were widely deposited.|
38064|Blue Whale Supersequence|71618|6|Mentioned|p131|Cenomanian|Albian|Of Bight Basin, Madura Shelf..||||||05-SEP-19
73234|Bremer 1|63241|4|Described|Pg. 14|||The Bremer 1 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||08-MAY-07
73234|Bremer 1|70067|5|Briefly described|Regional: Fig.3|Kimmeridgian|Oxfordian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to Sea Lion Supersequence.||
73235|Bremer 2|63241|4|Described|Pg. 15|||The Bremer 2 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||08-MAY-07
73235|Bremer 2|70067|5|Briefly described|Regional: Fig.3|Tithonian|Tithonian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to Minke Supersequence.||
73236|Bremer 3|63241|4|Described|Pg. 16|||The Bremer 3 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||
73236|Bremer 3|70067|5|Briefly described|Regional: Fig.3; p3|Valanginian|Berriasian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank. Differing seismic interpretations agree on this unit's potential as a source.||||Equivalent to Southern Right Supersequence and bottom-most Bronze Whaler Supersequence.||
73237|Bremer 4|63241|4|Described|Pg. 18|||The Bremer 4 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||08-MAY-07
73237|Bremer 4|70067|5|Briefly described|Regional: Fig.3|Aptian|Valanginian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to middle part of Bronze Whaler Supersequence.||
73238|Bremer 5|63241|4|Described|Pg. 19|||The Bremer 5 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||
73238|Bremer 5|70067|5|Briefly described|Regional: Fig.3|Cenomanian|Aptian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to White Pointer, Blue Whale, and upper half of Bronze Whaler Supersequences.||
73239|Bremer 6|63241|4|Described|Pg. 20|||The Bremer 6 unit is described in Chapter 2: Stratigraphic Framework of GA Record 2005/21.||||||
73239|Bremer 6|70067|5|Briefly described|Regional: Fig.3|Maastrichtian|Turonian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to Tiger and Hammerhead Supersequences.||
38065|Bronze Whaler Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Borda Formation.||||||
38065|Bronze Whaler Supersequence|61544|6|Mentioned|p367 Fig.3. |Albian|Valanginian|Ceduna Sub-basin. Post-rift slow thermal subsidence.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Early Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Albian|Valanginian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lacustrine and fluvial environments. Displays good oil potential in the fine-grained lacustrine facies of this sequence. Excellent fault seal capacity for hydrocarbons.  Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61.||||Overlies the Southern Right Supersequence. Overlain by the Blue Whale Supersequence. |Interbedded claystone, siltstone, snadstone and coal. |
38065|Bronze Whaler Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2|Albian|Valanginian|Bight Basin. Comprises all but the topmost part of Borda Formation. Potential reservoir.||||Overlies Southern Right Supersequence. Is overlain by Blue Whale Supersequence.||
38065|Bronze Whaler Supersequence|71618|6|Mentioned|p131|Albian|Valanginian|Of Bight Basin. Fluvial-lacustrine sedimentary succession.|140-100 Ma|||||
3707|Cartier Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Oligocene|Oligocene|Mory (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Comprises claystones, marls and calcisiltites.||||||01-MAR-10
3707|Cartier Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Neogene|Browse Basin.||||Overlies Grebe and Prion Formations. Is overlain by Oliver Formation.||
3707|Cartier Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60, p410|Oligocene|Eocene|Up to 290m thick; restricted to outer part of Bonaparte Basin.||||Overlies Hibernia Formation (disconformably).|Shale, minor marl and limestone.|
3707|Cartier Formation|13353|6|Mentioned|p401 Fig.2.|Neogene|Paleogene|||||Overlies Grebe and Prion Formations. Is overlain by Oliver Formation.||
3707|Cartier Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Neogene|Unit of Woodbine Group. Overlies Grebe and Prion Formations and underlies Oliver Formation.||91||||28-OCT-14
3707|Cartier Formation|24218|5|Briefly described|p850|Oligocene|Oligocene|Geological Province: Bonaparte Basin.||||||
3707|Cartier Formation|41437|6|Mentioned|Fig.3|||||||||
3707|Cartier Formation|41532|4|Described|p309|||||||||
3707|Cartier Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
3707|Cartier Formation|42442|3|Fully described|p31|Aquitanian|Oligocene|Age Oligocene to earliest Miocene (Aquitanian).||||||14-APR-08
3707|Cartier Formation|43699|6|Mentioned|Fig.6,p10|Miocene|Oligocene|||||||
3707|Cartier Formation|49637|5|Briefly described|Fig. 3|Miocene|Oligocene|Geological Province: Ashmore Platform.||||||07-FEB-11
3707|Cartier Formation|61548|6|Mentioned|p480 Fig.3|Oligocene|Oligocene|Northern Bonaparte Basin.||||||
3707|Cartier Formation|62837|5|Briefly described|Stratigraphic columns|Oligocene|Oligocene|Age: ~30Ma. Geological Province: Ashmore Platform and Northern Bonaparte Basin.||||||01-MAR-10
3707|Cartier Formation|63358|5|Briefly described|p4 Fig. 1.3|Miocene|Oligocene|||||||01-MAR-10
3707|Cartier Formation|64695|5|Briefly described|p262 |Late Oligocene|Late Oligocene|Occurs to the N and NW of the Fohn-1 region; not in this study area.||||Overlies Prion Formation. Is overlain by Oliver Formation.||
3707|Cartier Formation|65680|6|Mentioned|p709 Fig.2.|Chattian|Chattian|||||Unconformably overlies Hibernia Formation. Is overlain by Oliver Formation.||
3707|Cartier Formation|66187|5|Briefly described|p423|Oligocene|Oligocene|||||||
3707|Cartier Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Oligocene|Oligocene|||||||
3707|Cartier Formation|69297|5|Briefly described|p305|Aquitanian|Chattian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlain by the Oliver Formation.||
3707|Cartier Formation|69452|5|Briefly described|p36:15|Neogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
3707|Cartier Formation|70061|5|Briefly described|Regional geology; Figs.6-7. Sahul: Fig.2|Miocene|Oligocene|See also Vulcan: p3. Hydrocarbon reservoir in Vulcan Sub-basin.||Woodbine Group.||Overlies Prion Formation. Is overlain by Oliver Formation. Equivalent to Oliver Sandstone Member.||12-JUL-16
3707|Cartier Formation|70064|5|Briefly described|Regional Fig. 6. Central Fig.2|Miocene|Oligocene|See also Northern: Fig.2. Yampi: Fig.2. Brecknoff-Scott Reef Trend and Prudhoe Terrace, Browse Basin.||Woodbine Group.||Is overlain by Oliver Sandstone Member or Oliver Formation.||12-JUL-16
3727|Cascade Basalt|31571|2|Defined|p244|Pliocene|Pliocene|||||||
3727|Cascade Basalt|61942|5|Briefly described|p244|Pliocene|Pliocene|Norfolk Island. Nonfragmental lenticular flows. Tuff at base. Overlies: Duncombe Bay Basalt. Thickness: 60m+. Age: 2.74-2.41 +/- 0.03My from K/Ar and palaeomagnetic studies. Underlies Steels Point Basalt.||||||27-JAN-11
80796|Charlotte Supersequence|71958|2|Defined|p40-p41, p45-p46|Valanginian|Late Berriasian|Vlaming Sub-basin. The name is derived from the Charlotte Sandstone with which it largely coincides. The type locality is defined in Charlotte 1 (-31.80879499, 115.45037501) between 1574.4 and 2163.4 m (total thickness of 589m). Sequence stratigraphy. Fluvial to deltaic succession on the basis of palynology. Penetrated in six wells in the basin. Deposited over approximately 1.3 million years. Features the diagnostic fossils F. tumida, B. eneabbaensis, P. charlottensis, P. punctate, T. baculata, ?Moorodinium sp. (Helby et al, 1987 and Partridge 2006). This unit has a similar thickness and extent to the Charlotte sandstone. This supersequence is present in Bouvard 1, Charlotte 1, Minder Reef 1, Mullaloo 1, Parmelia 1 and Peel 1 and exhibits westward thickening growth wedge geometry in the Bathurst syncline. The base of this unit is equivalent to the major sequence boundary "126" (Haq et al., 1987), the top of E. torynum of Helby et al (1987) and near top "TS K1" sequence of Seggie (1990). See also p48-p50, p80-p83, p87, p91, p101.||||Unconformably overlain by the South Perth Supersequence (Warnbro Megasequence). Unconformably overlies the Hawley Member of the Carnac Formation.|Very fine to very couarse quartzose sandstone with minor interbedded mudstone and coal.|
73284|Crayfish Supersequence|63134|2|Defined|101|||||||||
73284|Crayfish Supersequence|63269|5|Briefly described|p605, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Oil-source correlation.|||Casterton Formation and Crayfish Subgroup.|Is overlain by Eumeralla Supersequence.||
73284|Crayfish Supersequence|69297|6|Mentioned|p77, p80, p81, p82, p96-p100, p110|Lower Cretaceous|Upper Jurassic|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. ||||||
73284|Crayfish Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25, p31||Early Cretaceous|See also p36-38, p40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Is overlain by Eumeralla Supersequence.|Argillaceous sandstone with interbedded claystone.|
73284|Crayfish Supersequence|70077|5|Briefly described|Nelson:p1. Regional: Fig.4; p3-4, p6, p9|Early Cretaceous|Early Cretaceous|Non-marine, fluvio-lacustrine deposits (shales and coals). A thick growth wedge in the ENE-trending Nerita Trough. Good potential source rocks.||||||
73284|Crayfish Supersequence|70078|6|Mentioned|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts Austral 1 and part of Austral 2 petroleum systems.||||||
73284|Crayfish Supersequence|70880|5|Briefly described|p75-77, 82-83|Barremian|Tithonian|Otway Basin. Australia-Antarctica rifting produced E-W to NW-SE striking faults bounding horst-and-graben structures. Syn-rift deposition. Maximum thicknesses up to 5000m in northern onshore Basin.||||Is overlain unconformably by Eumeralla Supersequence.|Contains organic-rich mudstones, sandstones and some basalts.|
73284|Crayfish Supersequence|71266|5|Briefly described|p613-615, p617, p620, p622 Fig.10|Barremian|Tithonian|Contains the oldest known stratigraphic units in the Otway Basin. Syn-rift deposition. Up to 5000m thick in the northern, onshore part of the Basin. Affected by faults; their growth is discussed in great detail.||||Is overlain by Eumeralla Supersequence.|Organic-rich mudstones, sandstones and basalts.|
38055|Dugong Supersequence|23792|5|Briefly described|p47, Fig.D4|||Equivalent to Wilsons Bluff Limestone. Geological Province: Bight Basin. Off shore. See also Dugong supersequence.||||||15-JUN-05
38055|Dugong Supersequence|24336|5|Briefly described|p99 Fig.3||Lutetian|Correlated to the Nullabor Limestone and Wilson Bluff Limestone.||||||
38055|Dugong Supersequence|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|Ceduna Sub-basin. Post-break-up thermal subsidence.||||Overlies Wobbegong Supersequence.||
38055|Dugong Supersequence|66578|6|Mentioned|p1007 Fig.4, p1010.|Quaternary|Paleogene|Ceduna Sub-Basin, Bight Basin.||||Overlies Wobbegong Supersequence.||
38055|Dugong Supersequence|69297|6|Mentioned|p14 fig 2.4, p25 fig 2.9|Tarantian|Ypresian|Eyre, Ceduna and Duntroon Sub-basins. Marls may be adequate sealing units. See also p26 fig 2.11, p43, p60,p61, p64.  ||||Overlies the Wobbegong Supersequence. |Includes marl and limestone. |
38055|Dugong Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2; p5|Holocene|Lutetian|Bight Basin. Comprises Nullarbor and Wilsons Bluff Limestones. Thick basal transgressive marls form a regional seal (for Hammerhead and Wobbegong Supersequences).||||Overlies Wobbegong Supersequence.|Includes marls and limestones.|
5807|Duncombe Bay Basalt|31571|2|Defined|p244|Pliocene|Pliocene|||||||
5807|Duncombe Bay Basalt|61942|5|Briefly described|p244|Pliocene|Pliocene|Norfolk Island. Lava flow. Age: 2.69-2.66 +/- 0.04My from K/Ar and palaeomagnetic studies. Underlies: Cascade Basalt disconformably.||||||27-JAN-11
5943|Echuca Shoals Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 16|Early Cretaceous|Early Cretaceous|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Also on p222, p228 Fig. 18.||||||01-MAR-10
5943|Echuca Shoals Formation|7142|6|Mentioned|p350 Fig.4.|Early Cretaceous|Early Cretaceous|Browse Basin.||||Overlies Upper Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|13267|6|Mentioned|pp274-279.|Early Cretaceous|Early Cretaceous|Barremian to Aptian.||||Overlies Flamingo Group. Is overlain by Darwin Formation.||
5943|Echuca Shoals Formation|13353|5|Briefly described|p398, p417.|Early Cretaceous|Early Cretaceous|Includes hydrocarbon source rocks. Characteristics of the W3 Petroleum System of this unit: richness, expulsion, migration conduits, reservoir/traps, seal facies, risks/assumptions etc, are detailed on p417.||||Overlies Upper Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|13354|6|Mentioned|p375 Fig.6.|Early Cretaceous|Early Cretaceous|Unit of Bathurst Island Group. Overlies Upper Vulcan Formation of the Swan Group, and underlies Jamieson Formation.||115||||28-OCT-14
5943|Echuca Shoals Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Early Cretaceous|Bathurst Island Group.||||||01-MAR-10
5943|Echuca Shoals Formation|23356|5|Briefly described|26 Tab.2|Early Cretaceous|Early Cretaceous|||||||
5943|Echuca Shoals Formation|23376|4|Described|p229 Fig.2; p244|Barremian|Valanginian|Of Bonaparte Basin.||||||15-AUG-06
5943|Echuca Shoals Formation|23378|4|Described|p180 Fig.2, p202||Early Cretaceous|Of Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||01-MAR-10
5943|Echuca Shoals Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
5943|Echuca Shoals Formation|24207|4|Described|p213|Barremian|Hauterivian|See also Echuca Shoals. Predominantly an extensive claystone. Geological Province: Vulcan Sub-basin.||||||01-MAR-10
5943|Echuca Shoals Formation|24234|5|Briefly described|p287 Fig.3|Early Cretaceous|Early Cretaceous|See also Echuca Shoals. Geological Province: Bonaparte Basin.||||||
5943|Echuca Shoals Formation|24379|5|Briefly described|p17|||Overlain by Wangarlu Formation. Geological Province: North west shelf.||||||14-APR-08
5943|Echuca Shoals Formation|24427|5|Briefly described|p49|Cretaceous|Cretaceous|||||||
5943|Echuca Shoals Formation|42053|4|Described|p42|||||||||01-MAR-10
5943|Echuca Shoals Formation|42056|4|Described|p100|||||||||
5943|Echuca Shoals Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
5943|Echuca Shoals Formation|42861|6|Mentioned|p4|||||||||
5943|Echuca Shoals Formation|43826|6|Mentioned|Fig.2,p163||Early Cretaceous|||||||01-MAR-10
5943|Echuca Shoals Formation|60378|5|Briefly described|p95, Fig 2|Early Cretaceous|Early Cretaceous|Marine sediments. Petroleum seal.||||||
5943|Echuca Shoals Formation|60385|6|Mentioned|p269 to 271|Albian|Valanginian|Browse Basin.|||||Organic-rich, oil-prone marine shale.|
5943|Echuca Shoals Formation|60386|6|Mentioned|p302|Valanginian|Berriasian|Browse Basin, Bonaparte Basin. Distal shelf/basin.||||||
5943|Echuca Shoals Formation|60634|6|Mentioned|p1168 Fig.3. |Early Cretaceous|Early Cretaceous|||Unit in Bathurst Island Group.||Overlies Vulcan Formation. Is overlain by Jamieson Formation.||
5943|Echuca Shoals Formation|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Early Cretaceous|Northern Bonaparte Basin.||||||
5943|Echuca Shoals Formation|61550|6|Mentioned|p495 Fig.2. |Aptian|Berriasian|||Unit in Bathurst Island Group.||||
5943|Echuca Shoals Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Neocomian|Age: ~133-~114Ma. Geological Province:  Ashmore Platform.||||||01-MAR-10
5943|Echuca Shoals Formation|63358|5|Briefly described|p4 Fig. 1.3|Aptian|Valanginian|Mentions occur throughout the text. See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
5943|Echuca Shoals Formation|64689|5|Briefly described|p3, p8 Fig.7, p15-19, p20 Fig.20|Lower Cretaceous|Lower Cretaceous|Contains a previously interpreted oil system.||||||
5943|Echuca Shoals Formation|64696|6|Mentioned|p134, p138, p140 |||An important source interval in the Browse Basin. Source of a gas column in the Upper Vulcan Formation, in Kalyptea-1.||||||
5943|Echuca Shoals Formation|64697|5|Briefly described|p84 Fig.2|Early Cretaceous|Early Cretaceous|||||||
5943|Echuca Shoals Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Aptian|Valanginian|Bathurst Island Group. Underlies the Jamieson Formation, overlies the Upper Vulcan Formation. Mount Ashmore Dome. Deep water claystone.||||||
5943|Echuca Shoals Formation|68223|6|Mentioned|p178 Fig.3|Aptian|Valanginian|||||||
5943|Echuca Shoals Formation|69297|6|Mentioned|p303, p305, p309|Aptian|Berriasian|Barcoo and Seringapatam sub-basins of the Browse Basin. Transgressive and highstand depositional packages. May contain oil shows.  ||Bathurst Island Group||Overlies the Brewster Member of the upper Vulcan Formation. ||
5943|Echuca Shoals Formation|69452|4|Described|p36:8, 15, 22|Cretaceous|Cretaceous|Pattillo and Nicholls, (1990). Deposited widely across the Bonaparte Basin. Offshore. Originally the basal Valanginian-Aptian interval of the Darwin Formation. >250m thick. Shallow marine deposits.||Bathurst Island Group.||Unconformably overlies Flamingo Group. Is overlain conformably by Darwin Formation.|Glauconitic claystone and siltstone.|12-JUL-16
5943|Echuca Shoals Formation|69456|5|Briefly described|p40:5|Early Cretaceous|Early Cretaceous|Bonaparte Basin. Valanginian-Barremian age.||Basal Bathurst Island Group.||||12-JUL-16
5943|Echuca Shoals Formation|69653|5|Briefly described|p6, 8, 10, 26-27, 38, 41-43, 50-51, 53|Cretaceous|Cretaceous|Petrel Sub-basin. Shoreface deposits. Schematic (gamma ray) well sections. Composite well diagram. See also p61, 63.||Bathurst Island Group.||Overlies Sandpiper Sandstone. Is overlain by Darwin Formation.|Medium-grained glauconitic sandstone with shale; mudstone interbedded with glauconitic siltstone/sandstone; mudstone with glauconitic sandstone. Facies described in detail.|
5943|Echuca Shoals Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Browse, Bonaparte Basins.||||Overlies Upper Vulcan Formation. Is overlain by Lower Jamieson Formation.||
5943|Echuca Shoals Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Aptian|Valanginian|See also Regional geology: Figs.6-7, p6, p10, p12, p14. Sahul: Fig.2, p1-3. Vulcan: Fig.2, p3. Potential source of wet gas and some light oil, such as that reservoired in the Darwin Formation. Forms a regional seal for hydrocarbons in the Vulcan Sub-basin, Sahul Syncline and N Bonaparte Basin. Source rock in Sahul Syncline.||Bathurst Island Group.||Overlies Sandpiper Sandstone. Is overlain by Darwin Formation.|Includes claystones.|12-JUL-16
5943|Echuca Shoals Formation|70064|5|Briefly described|Regional Fig.6; p4-7. Central:Fig.2;p1-2|Aptian|Valanginian|See also Northern: Fig.2; p1-2. Yampi: Fig.2; p1-2. Browse Basin. Contains organic-rich (mainly marine algae and bacteria) rocks with fair to moderate oil potential, and shallow marine sandstones and fans are potential reservoirs. It is also a regional seal (thick claystones). Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoirs in horsts and tilted fault-blocks.||Bathurst Island Group.||Overlies Upper Vulcan Formation. Is overlain by Lower Jamieson Formation.||12-JUL-16
73285|Eumeralla Supersequence|63134|2|Defined|101|||||||||
73285|Eumeralla Supersequence|63269|5|Briefly described|p605-606, p609, p616, p618, p622-624|Early Cretaceous|Early Cretaceous|Otway Basin. Most oil-prone coals and shales are near the base. Oil-source correlation.|<115 Ma.|||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.||
73285|Eumeralla Supersequence|69297|6|Mentioned|p77, p80, p81, p83, p96-p101|Lower Cretaceous|Lower Cretaceous|Nelson Sub-basin of the Otway Basin. Deposited in a fluvial or lacustrine environment. Interpreted from seismic data. See also p110, p114, p120, p370.||||||
73285|Eumeralla Supersequence|69651|5|Briefly described|p6, p10, p12-15, p17-19, p23, p25-26,p31|Albian|Early Cretaceous|See also p36-40, p42-44, p47, p49-50. Krassay et al. (2004). Otway Basin. Part of the Otway Supergroup. Potential source rocks. Fluvial to lacustrine deposits. Modelling diagrams.||||Overlies Crayfish Supersequence. Is overlain by Shipwreck Supersequence.|Argillaceous sandstone with interbedded claystone.|17-JUN-20
73285|Eumeralla Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p3-4, p6-7|Early Cretaceous|Early Cretaceous|See also Regional: p9, p11 . Non-marine, fluvio-lacustrine deposits. A thick growth wedge in the ENE-trending Nerita Trough. Good potential source and reservoir rocks. Sealed by Eumeralla Formation shales both laterally and vertically.||||||
73285|Eumeralla Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Early Cretaceous|Early Cretaceous|Hosts part of Austral 2 petroleum system in Otway Basin. Seismic interpretation suggests it is present in the Sandy Cape Sub-basin.||||Is overlain by Shipwreck Supersequence.|Fluvial and lacustrine rocks, including coaly facies.|
73285|Eumeralla Supersequence|70880|5|Briefly described|p76-77, 81-83|Albian|Aptian|Otway Basin. Thins to the W and N. The likely source rock for gas accumulations in eastern Otway Basin. Is ~2.3 km thick in onshore Victoria; thickens slightly to the S until the shelf-edge break where it noticeably thins. Top surface is a major Basin-wide unconformity.||||Unconformably overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Dominantly fluvio-lacustrine strata with a volcaniclastic sediment source.|
73285|Eumeralla Supersequence|71266|5|Briefly described|p614 Fig.3, p616-617, p620, p622 Fig.10|Early Cretaceous|Early Cretaceous|Otway Basin. Post-rift, thermal subsidence deposits. May be the source rock for gas accumulations in the eastern Otway Basin. Affected by faults; their growth is discussed in great detail.||||Overlies Crayfish Supersequence. Is overlain unconformably by Shipwreck Supersequence.|Fluvio-lacustrine deposits with evident volcaniclastic influence.|
6858|Fossil Head Formation|7142|6|Mentioned|p350 Fig.4.|Late Permian|Early Permian|Browse Basin.||||Overlies Kulshill Group. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|12466|5|Briefly described|p173.|||A hydrocarbon extract is a mature light paraffinic crude oil with no overt evidence for biodegradation; sourced from predominantly terrestrial organic matter deposited in estuaries.||||Overlies Keyling Formation. Is overlain by Hyland Bay Formation.||03-SEP-14
6858|Fossil Head Formation|12733|6|Mentioned|p565.|Early Permian|Early Permian|Bonaparte Basin. Gas-prone.||||||
6858|Fossil Head Formation|13194|4|Described|p382, p387, p396, p400, p405.|Kungurian|Artinskian|See Table 4-16, Figures 4-59, 4-60 and 4-71. Type Section: Tern 1 well (2993-3569m). 116-650m thick marine shelf deposits.||Kinmore Group||Overlies Keyling Formation (conformably). Overlain by Hyland Bay Formation.|Siltstone, mudstone, sandstone; minor limestone, and coal.|
6858|Fossil Head Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Kinmore Group.||||
6858|Fossil Head Formation|13234|6|Mentioned|p250 Fig.2, p252 Fig.4,p262 Tb.3,  |Permian|Permian|Proven reservoir and seal.||||Overlies Keyling Formation and Kulshill Group. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|13242|5|Briefly described|p214 Fig. 2, p215|Late Permian|Late Permian|Represents the base of Late Permian stratigraphy of the Bonaparte Basin. Formerly underlay Hyland Bay Formation; now underlies the Pearce Formation (Hyland Bay Sub-group). Geological Province: Bonaparte Basin. See also p226 Fig. 8.||||||07-FEB-11
6858|Fossil Head Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Late Permian|Early Permian|Bonaparte Basin. Unit of Kinmore Group. Overlies Kulshill Group and underlies Hyland Bay Formation. Equivalent to Poole Sandstone and Noonkanbah Formation in onshore Canning Basin.||180||||28-OCT-14
6858|Fossil Head Formation|22663|5|Briefly described|NT97 -1-4 p2||Permian|||||||01-MAR-10
6858|Fossil Head Formation|23377|6|Mentioned|p212 Fig.5||Early Permian|Of Vulcan Sub-basin.||||||18-SEP-06
6858|Fossil Head Formation|23820|4|Described|p205|Early Permian|Early Permian|Geological Province: Bonaparte Gulf Basin.||||||
6858|Fossil Head Formation|24378|5|Briefly described|p14|Early Permian|Early Permian|Geological Province: Bonaparte Basin.||||||
6858|Fossil Head Formation|24569|5|Briefly described|p248 Fig. 3|Early Permian|Early Permian|Of the Kinmore Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
6858|Fossil Head Formation|40077|6|Mentioned|Table 1|||||||||
6858|Fossil Head Formation|41532|3|Fully described|p301|||||||||
6858|Fossil Head Formation|41690|5|Briefly described|p5|||||||||
6858|Fossil Head Formation|41731|5|Briefly described|p517|||||||||
6858|Fossil Head Formation|41733|6|Mentioned|Fig.3|||||||||
6858|Fossil Head Formation|41839|6|Mentioned|p33|||||||||
6858|Fossil Head Formation|41864|6|Mentioned|p147|||Probably informal use of name||||||
6858|Fossil Head Formation|42055|4|Described|Fig.1 P52|||||||||
6858|Fossil Head Formation|42442|3|Fully described|p17|Kungurian|Artinskian|Microflora constrains age. Granulatispoities trisinus, Praecolpatites sinuosus, and near the top Mirobaculispora villosa.||||||20-SEP-18
6858|Fossil Head Formation|43661|6|Mentioned|Fig.3|||||||||
6858|Fossil Head Formation|43699|6|Mentioned|Fig.6,p10||Permian|||||||
6858|Fossil Head Formation|43739|6|Mentioned|Fig.5,p38||Early Permian|||||||
6858|Fossil Head Formation|49637|5|Briefly described|Fig. 3|Late Permian|Late Permian|Of the Kinmore Group. Geological Province: Petrel Sub-basin.See also Fig. 6.||||||07-FEB-11
6858|Fossil Head Formation|60386|6|Mentioned|p297, 310||Artinskian|Petrel Sub-basin, Roebuck/Canning Basin. Proximal shelf. ||||||
6858|Fossil Head Formation|60701|5|Briefly described|p12, p13|Permian|Permian|Forms the oil reservoir seal for the Keyling Formation. Geological Province: Bonaparte Basin.||||||10-APR-08
6858|Fossil Head Formation|62837|5|Briefly described|Stratigraphic columns|Early Permian|Early Permian|Of the Kinmore Group.  Age: ~287-~273Ma. Geological Province:  Western Bonaparte Basin, Northern Bonaparte Basin and Petrel Sub-basin (offshore). .||||||01-MAR-10
6858|Fossil Head Formation|64630|5|Briefly described|p31 Fig.2|Kungurian|Artinskian|Province: Bonaparte Basin. Underlies the Pearce Formation, overlies the Kulshill Group and Keyling Formation.  Palynology age: D. byroensis to M. villosa.||||||24-NOV-09
6858|Fossil Head Formation|64690|5|Briefly described|p504 Fig.2 |Kungurian|Early Permian|||||Is overlain by Pearce Formation.||
6858|Fossil Head Formation|64692|6|Mentioned|p522 Fig.2 |Late Permian|Permian|Bonaparte Basin.||||||
6858|Fossil Head Formation|64694|6|Mentioned|p235 Fig.3, p245 Fig.9|||Acts as seal for Keyling Formation.||||Overlies Keyling Formation. Is overlain by Hyland Bay Formation.||
6858|Fossil Head Formation|67354|5|Briefly described|p72, p73, pp96-97.|Artinskian|Sakmarian|A marine transgression blanketing the region with marine shales.||||Overlies, unconformably to conformably (in the north) the Keyling Formation.|Marine shales.|
6858|Fossil Head Formation|67370|6|Mentioned|p314 Fig.3, p316 Fig.5, p332. |Permian|Permian|||Basal unit in Kinmore Group.||Is overlain by Torrens Formation of Hyland Bay Subgroup.||
6858|Fossil Head Formation|69452|4|Described|p36:8, 11, 15, 18-20|Roadian|Sakmarian|Bhatia et al. (1984). Equivalent to Fossil Head beds of Caye (1968). Petrel Sub-basin, Bonaparte Basin. Marine shelf deposits. Lower part may be prodeltaic. Offshore and onshore. Up to 590m thick.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group) unconformably to conformably (in north). Is overlain unconformably by Pearce Formation (Hyland Bay Subgroup).|Carbonaceous siltstone and mudstone with sandstone and minor limestone. Abundantly fossiliferous.|12-JUL-16
6858|Fossil Head Formation|69454|5|Briefly described|p38:4|Roadian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Hyland Bay Subgroup.||||12-JUL-16
6858|Fossil Head Formation|69653|6|Mentioned|p10|Cisuralian|Cisuralian|Petrel Sub-basin.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group). Is overlain by Torrens Formation.||
6858|Fossil Head Formation|69673|5|Briefly described|p153 fig 125, p170 fig 142, p173|Artinskian|Sakmarian|590m thick. Age derived from fossil assemblage.||Kinmore Group||Overlain by Torrens Formation, overlies Keyling Formation|Carbonaceous siltstone and mudstone with sandstone and minor limestone.|
6858|Fossil Head Formation|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3|Roadian|Sakmarian|See also Regional geology: Figs.6-8, p11. Sahul: p2. Vulcan: Fig.2, p2. Regional seal for underlying Keyling Formation. Gas is reservoired in sandstone. Source rock in Sahul Syncline and Vulcan Sub-basin.||Kinmore Group.||Overlies Keyling Formation (Kulshill Group). Is overlain by Torrens Formation (Hyland Bay Subgroup).||12-JUL-16
6858|Fossil Head Formation|70774|5|Briefly described|p5 fig 3|Kungurian|Artinskian|Bonaparte Basin.||||||
6858|Fossil Head Formation|71146|5|Briefly described|p6|Kungurian|Sakmarian|Bonaparte Basin.||||Overlain by the Hyland Bay Subgroup.|Mudstone.|
6858|Fossil Head Formation|71623|6|Mentioned|p346 fig 4, p345 fig 2|Kungurian|Kungurian|Bonaparte Basin. Same as Lower Marine Beds of Dickens et al. (1972)? See also p344.|||||Shale|
6858|Fossil Head Formation|72505|5|Briefly described|p890|Roadian|Artinskian|Southern Bonaparte Basin. Correlated with the Striatopodocarpites fusus zone to the Microbaculispora villosa zone.||||Overlies the Keyling Formation and the Flat Top Limestone. Overlain by the Torrens Formation.||
6858|Fossil Head Formation|73117|6|Mentioned|p15|Kungurian|Sakmarian|Bonaparte Basin, southern.||||Underlain by Keyling Formation (Kulshill Group). Underlain by and equivalent to Flat Top Limestone.||
75612|Gibson Formation (OFF)|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228 Fig. 18|Late Cretaceous|Late Creatceous|In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||
75612|Gibson Formation (OFF)|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Late Cretaceous|Browse Basin.||||||
75612|Gibson Formation (OFF)|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Late Cretaceous|||||||
75612|Gibson Formation (OFF)|22663|5|Briefly described|AC97 1-4 Fig.4||Cretaceous|Of the Bathurst Island Group.||||||
75612|Gibson Formation (OFF)|23378|5|Briefly described|p180 Fig.2||Late Cretaceous|Invalid name - not the same unit as another Gibson Formation in the Yeelirrie area of WA which is properly defined and has priority. Of Bathurst Island Group, Vulcan Sub-basin.||||||20-SEP-14
75612|Gibson Formation (OFF)|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province: Vulcan Sub-Basin||||||20-SEP-14
75612|Gibson Formation (OFF)|24207|5|Briefly described|p218, p209 Fig. 5|Early Cretaceous|Early Cretaceous|Geological Province: Vulcan Sub-basin.||||||
75612|Gibson Formation (OFF)|42053|5|Briefly described|Fig.2 P29|||||||||
75612|Gibson Formation (OFF)|42066|5|Briefly described|Fig.3 P199|||||||||
75612|Gibson Formation (OFF)|43826|6|Mentioned|Fig.2,p163||Late Cretaceous|||||||
75612|Gibson Formation (OFF)|60385|6|Mentioned|p270, p272 Fig 3, p276|Campanian|Cenomanian|Browse Basin.|||||Pelagic marl, hemipelagic marl, limestone.|
75612|Gibson Formation (OFF)|60634|6|Mentioned|p1168 Fig.3.|Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Woolaston Formation. Is overlain by Fenelon Formation.||
75612|Gibson Formation (OFF)|61548|6|Mentioned|p480 Fig.3|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||||
75612|Gibson Formation (OFF)|61550|6|Mentioned|p495 Fig.2.|Late Cretaceous|Late Cretaceous|||Unit in Bathurst Island Group.||Overlies Woolaston Formation. Is overlain by Fenelon Formation.||
75612|Gibson Formation (OFF)|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Age: ~86-~82Ma. Geological Province: Vulcan Sub-basin, Londonderry High and Northern Bonaparte Basin.||||||
75612|Gibson Formation (OFF)|63358|5|Briefly described|p4 Fig. 1.3|Campanian|Santonian|||||||
75612|Gibson Formation (OFF)|64695|5|Briefly described|p262 Fig.8|Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Overlies Woolaston Formation. Is overlain by Fenelon Formation.||
75612|Gibson Formation (OFF)|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Campanian|Turonian|Bathurst Island Group. Underlies the Fenelon Formation, overlies the Woolaston Formation. Mount Ashmore Dome. Deep water limestone.||||||
75612|Gibson Formation (OFF)|68223|6|Mentioned|p178 Fig.3|Santonian|Santonian|||||||
38060|Hammerhead Supersequence|23792|5|Briefly described|p47|Late Cretaceous|Late Cretaceous|Equivalent to Potoroo Formation. See also Hammerhead supersequence. Geological Provice: Bight Basin. Off shore.||||||04-MAY-05
38060|Hammerhead Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Potoroo Formation.||||||
38060|Hammerhead Supersequence|61544|6|Mentioned|p367 Fig.3. |Maastrichtian|Santonian|Ceduna Sub-basin. Post-break-up thermal subsidence.||||Overlies Tiger Supersequence. ||
38060|Hammerhead Supersequence|66578|5|Briefly described|pp1005-1007, p1010.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin. c.3.5km thick. Sand-rich, believed to have been deposited very quickly from a local source. Host to a Delta-Deepwater Fold-Thrust Belt formed by gravity gliding, driven primarily by sediment supply, not gradient.||||Overlies Tiger Supersequence. Is overlain unconformably by Wobbegong and Dugong Supersequences.||
38060|Hammerhead Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Danian|Campanian|Ceduna and Duntroon Sub-basins. Maximum thickness of approximately 5000m. See also p37, p38, p41-p44, p46, p58, p60, p61.  ||||||
38060|Hammerhead Supersequence|70067|5|Briefly described|Ceduna: Fig.2;p1-2. Regional: Fig.2;p2-5|Maastrichtian|Santonian|Bight Basin. Comprises Potoroo Formation. Deltaic and shallow marine sandstones are potential oil and gas reservoirs according to petroleum systems modelling; marine shales are intraformational seals. Also sealed by thick transgressive marls at the base of the Dugong Supersequence.||||Overlies Tiger Supersequence. Is overlain by Wobbegong Supersequence.|Includes deltaic sandstones.|
73300|Heytesbury Supersequence|63134|2|Defined|112|||||||||
73300|Heytesbury Supersequence|63269|5|Briefly described|p605|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|69297|6|Mentioned|p80, p110, p111|||||||||
73300|Heytesbury Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Miocene|Oligocene|See also p44-47, p49-50. Open marine deposits. Possible seals. Modelling diagrams.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73300|Heytesbury Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
73300|Heytesbury Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Miocene|Oligocene|||||Unconformably overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Shelfal marls and limestones.|
73300|Heytesbury Supersequence|70880|5|Briefly described|p77|Miocene|Oligocene|Otway Basin. Open marine environment.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.|Mixed carbonate/siliciclastic sediments.|
73300|Heytesbury Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Miocene|Oligocene|Otway Basin.||||Overlies Nirranda Supersequence. Is overlain by Whalers Bluff Supersequence.||
79267|Heywood Formation|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Browse Basin.||||Overlies Upper Vulcan Formation.||
79267|Heywood Formation|70064|5|Briefly described|Regional p6. Yampi: p2|Albian|Albian|See also [...?]. Lower to upper shoreface marine sediments are potential reservoirs, while claystones are potential intraformational seals. Hosts the Cornea oil and gas accumulation on the Yampi Shelf.|||||Fine- to very fine-grained sandstones.|12-JUL-16
27432|Hibernia Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Eocene|Eocene|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
27432|Hibernia Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cenozoic|Cenozoic|Up to 1300m thick. Thickest in Vulcan Graben and Ashmore Platform.||||Overlain by Cartier Formation (disconformably). Overlies Bathurst Island Group.|Limestone, sandstone; minor shale and marl.|
27432|Hibernia Formation|13224|6|Mentioned|p485 fig 3|Oligocene|Paleocene|||||||
27432|Hibernia Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Eocene|Of the Woodbine Group.||||||26-SEP-06
27432|Hibernia Formation|23377|6|Mentioned|p212 Fig.5||Eocene|Of Vulcan Sub-basin.||||||26-SEP-06
27432|Hibernia Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
27432|Hibernia Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
27432|Hibernia Formation|41437|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|41532|4|Described|p308|||Mention Fig.15.||||||26-SEP-06
27432|Hibernia Formation|41690|6|Mentioned|p6|||||||||
27432|Hibernia Formation|41733|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|42034|4|Described|Fig.4 P11|||||||||
27432|Hibernia Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
27432|Hibernia Formation|42057|6|Mentioned|Fig.3 P70|||||||||
27432|Hibernia Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
27432|Hibernia Formation|42081|5|Briefly described|Fig.2 P291|||||||||
27432|Hibernia Formation|42151|6|Mentioned|Fig.3 P57|||||||||
27432|Hibernia Formation|42442|3|Fully described|p30|Eocene|Paleocene|||||||
27432|Hibernia Formation|43699|6|Mentioned|Fig.6,p10|Eocene|Paleocene|||||||
27432|Hibernia Formation|43707|5|Briefly described|Fig.3,p4-5||Tertiary|||||||
27432|Hibernia Formation|43739|6|Mentioned|Fig.5,p38|Oligocene|Paleocene|||||||
27432|Hibernia Formation|49637|5|Briefly described|Fig. 3|Eocene|Paleocene|Includes the Grebe Sandstone Member. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
27432|Hibernia Formation|60634|6|Mentioned|p1168 Fig.3. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|61155|5|Briefly described|p15, p16|Early Oligocene||See also Hibernia Formation. Age: >32.5Ma. Max. thickness: 1200m in Sahul Platform region. Geological Province: Bonaparte Basin / Ashmore and Sahul Platforms, Vulcan and Petrel Sub-basins; and Money Shoal Basin - north. ||||||
27432|Hibernia Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
27432|Hibernia Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: ~50-~42Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||22-JAN-07
27432|Hibernia Formation|64695|5|Briefly described|p260, p261 Fig.6, p262 Fig.8|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Grebe Formation. Is overlain by Prion Formation, and unconformably by Oliver Formation.||
27432|Hibernia Formation|64697|5|Briefly described|p84 Fig.2 |Eocene|Eocene|||||||
27432|Hibernia Formation|65680|6|Mentioned|p709 Fig.2.|Priabonian|Lutetian||||Includes Grebe Sandstone Member.|Overlies Johnson Formation. Is unconformably overlain by Cartier Formation and Oliver Sandstone Member.||
27432|Hibernia Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Eocene|Paleocene|Unit in the Woodbine Group. Underlies the Prion Formation, overlies the Grebe Formation. Mount Ashmore Dome. Limestone dominated with claystone at the base.||||||
27432|Hibernia Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
27432|Hibernia Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.|Grebe Sandstone Member.|||12-JUL-16
27432|Hibernia Formation|69673|6|Mentioned|p174|||||||||
27432|Hibernia Formation|70061|5|Briefly described|Regional geology Figs.6-7, p12|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.|Grebe Sandstone Member.|Overlies Johnson Formation. Is overlain by Prion Formation.||12-JUL-16
77685|Hyland Bay Subgroup|69452|5|Briefly described|p36:8, 15, 19-20|||Hughes (1978); redefined in Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Up to c.2300m thick collectively.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Is overlain unconformably by Mount Goodwin Subgroup.|Mudstone, siltstone, sandstone and carbonate rocks.|12-JUL-16
77685|Hyland Bay Subgroup|69454|5|Briefly described|p38:4|Changhsingian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kinmore Group.|Fossil Head, Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Overlies Kulshill Group. Is overlain by Mount Goodwin Subgroup.||12-JUL-16
77685|Hyland Bay Subgroup|69673|5|Briefly described|p153 fig 125, p173|||2300m thick.||Kinmore Group|Includes Torrens Formation, Pearce Formation, Cape Hay Formation, Dombey Formation, Tern Formation||Mudstone, siltstone, sandstone and carbonate rocks.|
77685|Hyland Bay Subgroup|70061|4|Described|Petrel Sub-basin; Figs.2 & 3, p2|Changhsingian|Roadian|See also Regional geology: Figs.6-8, p8-11, p13, p15-16, p19. Vulcan: Fig.2, p2. Hydrocarbon source. Pro-delta, shoreface and open marine sediments. Sealed by thick marine shales of Mount Goodwin Subgroup and Flamingo Group. Units in this Subgroup are now considered primary exploration targets in the central Petrel Sub-basin. Potential gas reservoir in Vulcan Sub-basin. Appears as Hyland Bay Formation on p19.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey and Tern Formations.|Overlies Fossil Head Formation. Is overlain by Mount Goodwin Subgroup.|Includes gas-prone shales.|12-JUL-16
77685|Hyland Bay Subgroup|71146|5|Briefly described|p6,  p43 fig 33|Guadalupian|Guadalupian|Bonaparte Basin.||||Overlies the Fossil Head Formation. Overlain by the Mount Goodwin Subgroup.|Mixed sandstone, mudstone, carbonate and coal.|
8851|Jamieson Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p222||Early Cretaceous|Pattillo and Nicholls (1990). In figure, Fm = Formation. Thickness: 1400m. Geological Province: Bonaparte Basin. Monotonous succession of silty claystones, with occasional thin limestone or dolomite stringers.  Also on p228 Fig. 18.||||||01-MAR-10
8851|Jamieson Formation|7142|6|Mentioned|p350 Fig.4.|Late Cretaceous|Early Cretaceous|Browse Basin.||||Overlies Echuca Shoals Formation. Is overlain by Woolaston Formation.||
8851|Jamieson Formation|13267|6|Mentioned|pp277-278.|Early Cretaceous|Early Cretaceous|Contains clays. Acted as a seal for hydrocarbons escaping along faults in Elang and Plover Formations.||||Overlies Darwin Formation.||
8851|Jamieson Formation|13353|6|Mentioned|p401 Fig.2.|Late Cretaceous|Early Cretaceous|||||Overlies Echuca Shoals Formation. Is overlain by Woolaston Formation.||
8851|Jamieson Formation|13354|6|Mentioned|p375 Fig.6, p385.|Late Cretaceous|Early Cretaceous|Unit of Bathurst Island Group. Overlies Echuca Shoals Formation and underlies Woolaston Formation. Contains shales.||115||||28-OCT-14
8851|Jamieson Formation|23376|4|Described|p229 Fig.2; p244||Albian|Of Bonaparte Basin.||||||28-SEP-06
8851|Jamieson Formation|23378|6|Mentioned|p180 Fig.2||Cretaceous|Of Bathurst Island Group. In the Vulcan Sub-basin.||||||28-SEP-06
8851|Jamieson Formation|24171|5|Briefly described|p722 Fig. 3|Cretaceous|Cretaceous|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
8851|Jamieson Formation|24207|5|Briefly described|p215, p209 Fig. 5|Aptian|Aptian|Bathyal dark grey to black claystones are typical.  Unconformably overlies the Lower Vulcan Formation.  Max. thickness: 300m (in Londonderry High area).  Geological Province: Vulcan Sub-basin.||||||28-SEP-06
8851|Jamieson Formation|24234|5|Briefly described|p287 Fig.3|Albian|Albian|Overlies Darwin Formation. Geological Province: Bonaparte Basin.||||||
8851|Jamieson Formation|42053|4|Described|p43|||See also Fig.2 p29.||||||01-MAR-10
8851|Jamieson Formation|42056|5|Briefly described|p98|||||||||
8851|Jamieson Formation|42861|6|Mentioned|p4|||||||||
8851|Jamieson Formation|43826|6|Mentioned|Fig.2,p163|Late Cretaceous|Early Cretaceous|||||||01-MAR-10
8851|Jamieson Formation|60385|6|Mentioned|p272 Fig 3, p277|Cenomanian|Aptian|Browse Basin. |||||Mudstone.|
8851|Jamieson Formation|60386|6|Mentioned|p302|Aptian|Barremian|Browse Basin. Distal shelf/basin.||||||
8851|Jamieson Formation|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Late Cretaceous|Early Cretaceous|||Unit in Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Puffin Formation.||
8851|Jamieson Formation|61548|6|Mentioned|p480 Fig.3|Cenomanian|Albian|Northern Bonaparte Basin.||||||
8851|Jamieson Formation|61550|6|Mentioned|p495 Fig.2. |||||Unit in Bathurst Island Group.||Is overlain by Woolaston Formation.||
8851|Jamieson Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Bathurst Island Group. Divided into Upper and Lower Jamieson Formation. Age: ~114-~95Ma. Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||01-MAR-10
8851|Jamieson Formation|63358|5|Briefly described|p4 Fig. 1.3|Cenomanian|Aptian|Mentions occur throughout the text. See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
8851|Jamieson Formation|64689|6|Mentioned|p18 Fig.19, p20 Fig.20|||||||Unconformably overlies Echuca Shoals Formation.||
8851|Jamieson Formation|64697|5|Briefly described|p84 Fig.2 |Late Cretaceous|Early Cretaceous|||||||
8851|Jamieson Formation|65078|6|Mentioned|p35|||Contains a clastic "basal transgressive sand" which indicates deltaics and general shallow marine geology. Geological province: Vulcan Sub-basin.||||||30-APR-09
8851|Jamieson Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Cenomanian|Albian|Bathurst Island Group. Underlies the Woolaston Formation, overlies the Echuca Shoals Formation. Mount Ashmore Dome. Deep water claystone.||||||
8851|Jamieson Formation|68223|6|Mentioned|p178-181 Figs. 3 - 6|Cenomanian|Albian|||||||
8851|Jamieson Formation|69297|5|Briefly described|p303, p305, p311|Turonian|Aptian|Barcoo Sub-basin of the Browse Basin. Misspelt as the Jamison Formation on p311.  ||Bathurst Island Group||Overlies the Echuca Shoals Formation. Overlain by the Woolaston Formation. |Mudstones or shales.|
8851|Jamieson Formation|69452|5|Briefly described|p36:15|Cretaceous|Cretaceous|Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
8851|Jamieson Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Cenomanian|Albian|See also Sahul: Fig.2. Vulcan: Fig.2-3. Presented also as Upper and Lower Jamieson Formations. May provide a top seal to Vulcan Sub-basin.||Bathurst Island Group.|||Includes claystones and marls.|12-JUL-16
8851|Jamieson Formation|70064|5|Briefly described|Regional p4-8. Central:p2. Northern:p1.|Early Cretaceous|Early Cretaceous|Central Caswell Sub-basin. Contains mixed marine and terrestrial organic matter with moderate to good source potential. Potential regional seal: claystone 500-600m thick across the Sub-basin. Mis-spelt as Jamison in Northern: p1.||||||12-JUL-16
75710|Jansz Sandstone|67970|5|Briefly described|p3, p13, p25 Fig.4.|Oxfordian|Oxfordian|Eastern Exmouth Plateau. Sandy shelfal facies. Reservoir in the supergiant Io/Jansz gas field. Hydrocarbon shows in Glencoe 1, Jansz 1 and Jansz 3 wells.||||Is overlain by Dingo Claystone.||
75710|Jansz Sandstone|68135|6|Mentioned|p51 fig 2a|Late Jurassic|Late Jurassic|[Mis-spelling of Jansz: appears as Janz]. Northern Carnarvon Basin.||||||14-SEP-17
75710|Jansz Sandstone|70066|5|Briefly described|Exmouth: Fig.2; p1-2. Regional: Fig.6;p6|Kimmeridgian|Oxfordian|Exmouth Plateau, Northern Carnarvon Basin. Significant petroleum reservoir: hosts the giant Io/Jansz gas accumulation.||||Overlies Athol Formation. Is overlain by Dingo Claystone.||
25092|Johnson Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Eocene|Paleocene|In figure, Fm = Formation. Geological Province: Bonaparte Basin. Interbedded carbonate lithologies.||||||01-MAR-10
25092|Johnson Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Paleocene|Woodbine Group.||||||01-MAR-10
25092|Johnson Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
25092|Johnson Formation|24218|5|Briefly described|p850|Paleocene|Paleocene|Geological Province: Bonaparte Basin.||||||
25092|Johnson Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25092|Johnson Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
25092|Johnson Formation|43826|6|Mentioned|Fig.2,p163||Paleogene|||||||01-MAR-10
25092|Johnson Formation|60385|4|Described|p272 Fig 3|Danian|Maastrichtian|Browse Basin. |||||Limestone, minor sandstone.|
25092|Johnson Formation|60634|6|Mentioned|p1168 Fig.3. |Palaeocene|Palaeocene|||Unit in Bathurst Island Group.||Overlies Puffin and Borde Formations. Is overlain by Grebe Formation.||
25092|Johnson Formation|61548|6|Mentioned|p480 Fig.3|Paleocene|Paleocene|Northern Bonaparte Basin.||||||
25092|Johnson Formation|61550|6|Mentioned|p495 Fig.2. |Paleocene|Paleocene|||Basal unit in Woodbine Group.||Overlies Puffin Formation. Is overlain by Grebe Formation.||
25092|Johnson Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Paleocene|Age: 65-~56Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
25092|Johnson Formation|64695|5|Briefly described|p262 Fig.8|Palaeocene|Palaeocene|Northern Bonaparte Basin.||||Overlies Wangarlu and Turnstone Formations.||
25092|Johnson Formation|64697|5|Briefly described|p84 Fig.2 |Paleocene|Palaeocene|||||||
25092|Johnson Formation|65680|6|Mentioned|p709 Fig.2.|Thanetian||||||Is overlain by Hibernia Formation.||
25092|Johnson Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Eocene|Paleocene|Unit in Woodbine Group. Underlies the Grebe Formation, overlies the Puffin Formation. Mount Ashmore Dome. Limestone dominated with claystone at base.||||||
25092|Johnson Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Paleocene|Paleocene|||||||
25092|Johnson Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
25092|Johnson Formation|69673|6|Mentioned|p174|||||||||
25092|Johnson Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Eocene|Paleocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2, p2-3. Carbonates of this unit seal Wangarlu and Puffin Formations exploration targets. Potential oil reservoir in Vulcan Sub-basin.||Woodbine Group.||Overlies Turnstone and Puffin Formations. Is overlain by Hibernia Formation.||12-JUL-16
25092|Johnson Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Paleocene|Paleocene|See also Northern: Fig.2. Brecknoff-Scott Reef Trend, Browse Basin.||Woodbine Group.||Overlies Puffin Formation. Equivalent to Bassett Formation.||12-JUL-16
9623|Kinmore Group|5952|5|Briefly described|p221 Fig. 15|Permian|Permian|Includes Hyland Bay Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
9623|Kinmore Group|13194|4|Described|p387 Tb. 4-16|Triassic|Permian|460-2000m thick.|||Mount Goodwin Formation|Overlies Kulshill Group (conformably).||
9623|Kinmore Group|13222|6|Mentioned|p229 Fig.2.|||Gorter (1998) omits Hyland Bay Formation and lists several Formations (not Members).|||Includes Fossil Head, Mount Goodwin and Hyland Bay Formations.|||
9623|Kinmore Group|13224|6|Mentioned|p485 fig 3|Scythian|Kazanian|||||||
9623|Kinmore Group|13242|5|Briefly described|p214 Fig. 2|Late Permian|Late Permian|Defined by Mory (1988, 1991) who included Fossil Head and Mount Goddwin Formations - excluded in this paper. Geological Province: Bonaparte Basin.||||||07-FEB-11
9623|Kinmore Group|13354|6|Mentioned|p375 Fig.6.|Permian|Late Carboniferous|Comprises, in ascending order, Kulshill Group, Fossil Head Formation and Hyland Bay Formation.||94||||28-OCT-14
9623|Kinmore Group|22663|5|Briefly described|AC97 1-4 Fig.4||Permian|||||||01-MAR-10
9623|Kinmore Group|24569|5|Briefly described|p248 Fig. 3|Triassic|Permian|Includes the Fossil Head, Hyland Bay and Mount Goodwin Formations. Geological Province: Petrel Sub-basin.||||||02-MAR-05
9623|Kinmore Group|41459|6|Mentioned|p283|||Reserved as Kinmore Member. See also Fig.2||||||
9623|Kinmore Group|41532|3|Fully described|p301|||||||||
9623|Kinmore Group|41689|6|Mentioned|Table 1|||||||||
9623|Kinmore Group|41731|6|Mentioned|Fig.3|||||||||
9623|Kinmore Group|42053|5|Briefly described|Fig.15 P46|||||||||01-MAR-10
9623|Kinmore Group|42055|4|Described|Fig.1 P52|||||||||
9623|Kinmore Group|42056|5|Briefly described|Fig.6 P95|||||||||
9623|Kinmore Group|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
9623|Kinmore Group|42075|5|Briefly described|Fig.4 P245|||||||||
9623|Kinmore Group|42442|3|Fully described|p17|Anisian|Artinskian|Equivalent to 'Port Keats Group' of Noakes 1949. Variation on Kinmore Group, WA.||||||03-AUG-06
9623|Kinmore Group|43661|6|Mentioned|Fig.3|||||||||
9623|Kinmore Group|43699|6|Mentioned|Fig.6,p10|Middle Triassic|Early Triassic|||||||
9623|Kinmore Group|43707|5|Briefly described|Fig.3,p4||Permian|||||||
9623|Kinmore Group|43739|6|Mentioned|p10||Permian|||||||
9623|Kinmore Group|49637|5|Briefly described|Fig.3|Early Triassic|Late Permian|Includes the Fossil Head, Hyland Bay and Mount Goodwin Formations. Geological Province: Petrel Sub-basin.||||||07-FEB-11
9623|Kinmore Group|60634|6|Mentioned|p1168 Fig.3. |Permian|Permian||||Includes Hyland Bay Formation.|Is overlain by Sahul Group.||
9623|Kinmore Group|62837|5|Briefly described|Stratigraphic columns|Early Triassic|Early Permian|Includes Fossil Head, Hyland Bay and Mount Goodwin Formations.  Age: ~287-~242 Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
9623|Kinmore Group|64698|4|Described|lithinterp table|Kungurian|Asselian|Age ~275-298Ma (Early Permian). Bonaparte Basin. Max. thickness 1800m. Succession of basal conglomerate followed by siltstone, silty sandstone, limestone and minor diamictite.||||||07-JAN-09
9623|Kinmore Group|67354|6|Mentioned|p73. |||Includes Permian and early Triassic strata that were formerly part of the Port Keats Group.||||||
9623|Kinmore Group|67370|5|Briefly described|p313 Fig.2, p332. |Triassic|Permian|Revised. Mount Goodwin Formation is raised to Subgroup rank.|||Includes the lower Fossil Head Formation, the middle Hyland Bay Subgroup and the upper Mount Goodwin Subgroup.|Is overlain by Troughton Group.||
9623|Kinmore Group|69297|6|Mentioned|p305, p322|Olenekian|Guadalupian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||||Overlain by the Sahul Group. ||
9623|Kinmore Group|69452|5|Briefly described|p36:4-5, 8, 15, 18-21|Middle Triassic|Permian|Mory (1991); redefined in Gorter (1998) and Gorter et al. (2009). Equivalent to Port Keats Group of Noakes (1949). Discontinuous outcrop; extensive in the subsurface.|||Mount Goodwin, Hyland Bay Subgroups; Fossil Head Formation.|Unconformably overlies Kulshill Group. Is overlain unconformably by Troughton Group.||12-JUL-16
9623|Kinmore Group|69454|5|Briefly described|p38:4|Olenekian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.|||Hyland Bay, Mount Goodwin Subgroups.|Overlies Kulshill Group. Is overlain by Troughton Group.||12-JUL-16
9623|Kinmore Group|69653|5|Briefly described|p10, 14-15|Triassic|Permian|Petrel Sub-basin. Tidal shelf environment, succeeded by shallow-marine transgressive sediments. Forms an extensive regional seal.|||Hyland Bay Sub-group; Mount Goodwin Sub-group; Fossil Head Formation.|Overlies Kulshill Group. Is overlain by Troughton Group.|Thick transgressive sequences of marine mudstones and siltstones, succeeded by shallow-marine sandstones, mudstones and carbonates, topped by marine shales and siltstones.|
9623|Kinmore Group|69673|6|Mentioned|p166 fig 136, p168 fig 138, p173|Triassic|Permian ||||Includes Fossil Head Formation, Hyland Bay Subgroup, Mount Goodwin Subgroup|Unconformably overlies Kulshill Group||
9623|Kinmore Group|70061|5|Briefly described|Petrel Sub-basin; Figs.2 & 3|Olenekian|Artinskian|See also Regional geology: Figs.6-8, p8. Sahul: p2. Vulcan: Fig.2, p2. Source rock in Sahul Syncline.|||Mount Goodwin, Hyland Bay Subgroups; Fossil Head Formation.|Overlies Kulshill Group. Is overlain by Troughton Group.||12-JUL-16
9623|Kinmore Group|70064|5|Briefly described|Regional Fig. 6. Central Fig.2; p2|Anisian|Sakmarian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins and Prudhoe Terrace, Browse Basin. Equivalent units in Central Caswell Sub-basin are potential reservoirs.|||Hyland Bay, Mount Goodwin Sub-groups.|Overlies Kulshill Group. Is overlain by Sahul Group.||12-JUL-16
9623|Kinmore Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone|
80794|Leederville Supersequence|71958|2|Defined|p38, p40-p41, p45-p46|Aptian|Barremian|Vlaming Sub-basin. Sequence stratigraphy. Partially incorporates the Leederville Formation after which it is named. The type locality occurs in Warnbro 1 (-32.23769, 115.347327) between 1489 and 1081.6m (total thickness of 407.4m). Age is derived by the presence of diagnostic microfossils including B. Jaegeri, O. operculata, F.monilifera and D. davidii Dinocyst zones. Highly fossiliferous in places. The maximum thickness penetrated by a well is 499.7m at Warnbro 1. Offshore the sequence is thickest in the southern Vlaming Sub-basin over the Southern Peel Arch in the Bathurst Syncline. In the northern Vlaming Sub-basin this unit is thickest in the east. Interpreted to have been deposited in a shallow marine to fluvial environment. See also p51, p54, p60-p62, p64-p65.||Warnbro Megasequence||Conformably overlies the South Perth Supersequence. Unconformably overlain by the Coolyena Megasequence.|Fine to very coarse-grained sandstones containing glauconite, mica and minor feldspar interbedded with pyritic, glauconitic argillaceous and micaceous mudstones. |
76874|Marligur Formation|67564|6|Mentioned|p52.|Cretaceous|Cretaceous|Money Shoal Basin.||||||
76874|Marligur Formation|69456|5|Briefly described|p40:2; 40:3 Fig.40.4; 40:4, 6-8|Cretaceous|Cretaceous|Mory (1988); formerly the Marligur Member of Hughes and Senior (1974). Money Shoal Basin. Up to 62m thick. Exposures are generally poor, deeply weathered and only a few metres thick. In many areas, is capped by surficial ferricrete above a mottled zone.||Bathurst Island Group.||Lateral equivalent of (and interfingers with) Darwin Formation.|Medium- to coarse-grained, poorly consolidated quartz sandstone, clayey sandstone and sandy claystone; thin basal quartzic conglomerate.|12-JUL-16
76874|Marligur Formation|69673|6|Mentioned|p204|Cretaceous|Cretaceous|20-63m thick.||Bathurst Island Group||Equivalent to Darwin Formation|Quartz sandstone, clayey sandstone and sandy claystone.|
76874|Marligur Formation|73083|6|Mentioned|p17|Cretaceous|Cretaceous|Money Shoal Basin.||||||
38067|Minke Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Echidna Formation.||||||
38067|Minke Supersequence|61544|6|Mentioned|p367 Fig.3. |Berriasian|Tithonian|Ceduna Sub-basin. Syn-rift mechanical extension.||||Overlies Sea Lion Supersequence. Is overlain by Southern Right Supersequence.||
38067|Minke Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Late Jurassic|Ceduna Sub-Basin, Bight Basin.||||Overlies Sea Lion Supersequence.||
38067|Minke Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Tithonian|Tithonian|Eyre, Ceduna and Duntroon Sub-basins. Shale facies within this sequence have the best potential to be seal rocks in the Eyre Sub-basin. Good faulting seal capacity for hydrocarbons. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61. ||||Overlies the Sea Lion Supersequence. Overlain by the Southern Right Supersequence. |Sandstone, siltstone and claystone. |
38067|Minke Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Berriasian|Tithonian|Bight Basin. Includes the Echidna Formation (except the topmost part); the lithologies are unknown, not having been penetrated by wells.||||Overlies Sea Lion Supersequence. Is overlain by Southern Right Supersequence.||
13374|Mullaloo Sandstone Member|12759|4|Described|p43; p28 Tb. 7; p32 Fig 15; P36 Fig 17|Eocene|Paleocene|Defined Quilty (1974). Type section in offshore Quinns Rock No.1 well, 20km W of Whitfords, (AMG Zone 50, 359480m E, 6480360m N) between 68-365 m depth. Max onshore thickness is 200m. Occupies deep marine channels incised into Kings Park Formation. Forms a minor confined aquifer.||At or near top of Kings Park Formation.|||Poorly sorted, fine- to very coarse-grained, pale brownish-green, slightly glauconitic and clayey sand.|12-MAY-14
13374|Mullaloo Sandstone Member|14227|5|Briefly described|Enclos. 2|Eocene|Eocene|Age: Early Eocene. Presented as Mullaloo Sandstone Mem.||||||07-FEB-11
13374|Mullaloo Sandstone Member|29693|6|Mentioned|Fig.7|||||||||
13374|Mullaloo Sandstone Member|31562|6|Mentioned|Fig. 3|||Member of Kings Park Formation.||||||15-JAN-08
13374|Mullaloo Sandstone Member|32748|2|Defined|p28|Tertiary|Tertiary|||||||
13374|Mullaloo Sandstone Member|32750|6|Mentioned|p307|||||||||
13374|Mullaloo Sandstone Member|34951|6|Mentioned|p115|||||||||
13374|Mullaloo Sandstone Member|36293|5|Briefly described|p197|||||||||
13374|Mullaloo Sandstone Member|44144|5|Briefly described|p503 Tb.4-21, p519|Early Eocene|Early Eocene|||Top of Kings Park Formation.|||Poorly sorted sandstone.|
13374|Mullaloo Sandstone Member|63745|5|Briefly described|p68, p78 Appx.|Eocene|Paleocene|At top of Kings Park Formation. Unconformably overlain by Perth Formation.||||||07-FEB-11
13374|Mullaloo Sandstone Member|68254|6|Mentioned|p1040 Tb.3|||Member status specified in heading of Table 3. See informal Mullaloo Sandstone in this paper.||||||
13374|Mullaloo Sandstone Member|68811|6|Mentioned|p180 tbl 39|Tertiary|Tertiary|||Of Kings Park Formation.||||15-APR-20
77110|Nancar Sandstone|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Late Jurassic|Northern Bonaparte Basin.||||||
77110|Nancar Sandstone|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Tithonian|Tithonian|||||||
73299|Nirranda Supersequence|63134|2|Defined|111-112|||||||||
73299|Nirranda Supersequence|63269|5|Briefly described|p605|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||Misspelt as the Nirrandra Supersequence on p98. ||||||
73299|Nirranda Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22-23, p29, p39|Oligocene|Eocene|See also p44-47, p49-50. Relatively thin and undeformed open marine deposits; marks a major marine transgression. Possible seals. Modelling diagrams.||||Overlies Wangerrip Supersequence conformably [!]. Is overlain by Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73299|Nirranda Supersequence|70077|5|Briefly described|Regional: Fig.4; p4-5|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
73299|Nirranda Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Oligocene|Eocene|Deposition was truncated by a major mid-Oligocene unconformity.||||Overlies Wangerrip Supersequence. Is overlain unconformably by Heytesbury Supersequence.|Shallow-marine sandstones, marls and limestones.|
73299|Nirranda Supersequence|70880|5|Briefly described|p77|Oligocene|Eocene|Otway Basin. Open marine environment.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.|Mixed carbonate/siliciclastic sediments.|
73299|Nirranda Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Oligocene|Eocene|Otway Basin.||||Overlies Wangerrip Supersequence. Is overlain by Heytesbury Supersequence.||
14550|Oliver Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p229|Pliocene|Miocene|In figure, Fm = Formation. Includes Oliver Sand Member. Geological Province: Bonaparte Basin. Composed of firm to moderately hard calcarenites with abundant skeletal material.||||||01-MAR-10
14550|Oliver Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Neogene|Browse Basin.||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13353|6|Mentioned|p401 Fig.2.|Neogene|Neogene|||||Overlies Cartier Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Neogene|Unit of Woodbine Group. Overlies Cartier Formation and underlies Barracouta Formation.||86||||28-OCT-14
14550|Oliver Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Miocene|Of the Woodbine Group.||||||01-MAR-10
14550|Oliver Formation|23377|4|Described|p212 Fig.5; p218|Quaternary|Miocene|In the Vulcan Sub-basin. Unconformable base.||||||21-NOV-06
14550|Oliver Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
14550|Oliver Formation|24218|5|Briefly described|p847|Early Miocene|Early Miocene|Geological Province: Bonaparte Basin.||||||
14550|Oliver Formation|42053|5|Briefly described|Fig.2 P29|||See also Fig.2||||||01-MAR-10
14550|Oliver Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
14550|Oliver Formation|60634|6|Mentioned|p1168 Fig.3. |Miocene|Miocene|||Unit in Woodbine Group.||Overlies Prion Formation. Is overlain by Barracouta Formation.||
14550|Oliver Formation|61548|6|Mentioned|p480 Fig.3|Miocene|Miocene|Northern Bonaparte Basin.||||||
14550|Oliver Formation|61550|6|Mentioned|p495 Fig.2. |||||Unit in Woodbine Group.||Is overlain by Barracouta Formation.||
14550|Oliver Formation|62837|5|Briefly described|Stratigraphic columns|Late Miocene|Oligocene|Contains the Oliver Sand Member. Age: ~25-~7.0Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
14550|Oliver Formation|63358|5|Briefly described|p4 Fig. 1.3|Miocene|Miocene|||||||01-MAR-10
14550|Oliver Formation|64695|5|Briefly described|p260-262  |Miocene|Miocene|Northern Bonaparte Basin.|||Includes Oliver Sandstone Member.|Unconformably overlies Prion and Hibernia Formations. Is overlain by Barracouta Formation.||
14550|Oliver Formation|64697|5|Briefly described|p84 Fig.2 |Miocene|Miocene|||||||
14550|Oliver Formation|65680|6|Mentioned|p709 Fig.2.|Messinian|Aquitanian|Host to an interpreted dish-shaped, multiringed impact structure, about 2.5 km diameter, formed by collision of a meteorite or small asteroid with unconsolidated, water-saturated shallow-marine shelf carbonate, in mid- to late-Serravallian.|||Includes Oliver Sandstone Member.|Overlies Cartier Formation. Is unconformably overlain by Barracouta Formation.||
14550|Oliver Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1, p421, p423|Miocene|Oligocene|Unit in Woodbine Group. Underlies Barracouta Formation (WA), overlies the Prion Formation unconformably. In the Mount Ashmore Dome. Mainly limestone and dolomite.||||||
14550|Oliver Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4, p184 Fig.9|Miocene|Miocene|In Fig. 9, the base of Pliocene is indicated by the Top Oliver Formation.||||||
14550|Oliver Formation|69297|6|Mentioned|p305|Messinian|Chattian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Woodbine Group||Overlies the Cartier Formation. Overlain by the Barracouta Shoal Formation.||
14550|Oliver Formation|69452|5|Briefly described|p36:15, 22|Neogene|Neogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
14550|Oliver Formation|69673|6|Mentioned|p174|||||||||
14550|Oliver Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Miocene|Oligocene|See also Sahul: Fig.2, p2. Vulcan: Fig.2, p2. Reservoir. Sealed by intraformational carbonates or the overlying Barracouta Shoal Formation.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
14550|Oliver Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Miocene|Oligocene|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin.||Woodbine Group.|Oliver Sandstone Member.|Overlies Cartier Formation. Is overlain by Barracouta Shoal Formation.||12-JUL-16
79265|Picard Shale""|69297|6|Mentioned|p339|Middle Jurassic|Middle Jurassic|Potential petroleum source rock.||||||
79265|Picard Shale""|70065|6|Mentioned|Regional: p5|Middle Jurassic|Middle Jurassic|Identified by Woodside Energy Ltd (2003; 2007) as a source rock with significant liquids potential, and being the inferred source of the Nebo 1 oil in the Beagle Sub-basin.||||||
15604|Prion Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p228|Eocene|Eocene|Pattillo and Nicholls (1990). In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
15604|Prion Formation|7142|6|Mentioned|p350 Fig.4.|Neogene|Paleogene|Browse Basin.||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13353|6|Mentioned|p401 Fig.2.|Paleogene|Paleogene|||||Overlies Bassett Formation. Is overlain by Cartier Formation.||
15604|Prion Formation|13354|6|Mentioned|p375 Fig.6.|Neogene|Palaeogene|Unit of Woodbine Group. Overlies Bassett Formation and underlies Cartier Formation.||83||||28-OCT-14
15604|Prion Formation|22663|5|Briefly described|AC97 1-4 Fig.4|Oligocene|Eocene|Of the Woodbine Group.||||||01-MAR-10
15604|Prion Formation|23378|6|Mentioned|p180 Fig.2||Eocene|Of the Woodbine Group. In the Vulcan Sub-basin.||||||27-NOV-06
15604|Prion Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province: Vulcan Sub-Basin.||||||20-SEP-14
15604|Prion Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
15604|Prion Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
15604|Prion Formation|42066|5|Briefly described|Fig.3 P199|||||||||
15604|Prion Formation|60634|6|Mentioned|p1168 Fig.3. |Oligocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation. Is overlain by Oliver Formation.||
15604|Prion Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
15604|Prion Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Hibernia Formation.||
15604|Prion Formation|62837|5|Briefly described|Stratigraphic columns|Oligocene|Eocene|Age: ~41-~33Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||01-MAR-10
15604|Prion Formation|63358|5|Briefly described|p4 Fig. 1.3|Oligocene|Eocene|||||||01-MAR-10
15604|Prion Formation|64695|5|Briefly described|p260, p262|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Hibernia Formation. Is overlain unconformably by Oliver Formation.||
15604|Prion Formation|66187|5|Briefly described|p413 Fig.2|Eocene||Unit in the Woodbine Group. Underlies the Oliver Formation unconformably; overlies the Hibernia Formation. Mount Ashmore Dome.||||||
15604|Prion Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
15604|Prion Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.||||12-JUL-16
15604|Prion Formation|69673|6|Mentioned|p174|||||||||
15604|Prion Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.||Overlies Hibernia Formation. Is overlain by Cartier Formation.||12-JUL-16
74206|Sandbar Sandstone|61542|5|Briefly described|p277 Fig. 2, p285|Visean|Visean|Newly added to the Weaber Group -  forms part of revision by authors. Overlain by Sunbird Fm.which may(?) truncate it, or it pinches out. Geological Province: onshore Bonapart Basin/offshore Petrel-Sub-basin. tyep section in offshore Sandbar-1.||||Overlain by Sunbrid Formation. Overlies Tanmurra Fm.||26-NOV-18
74206|Sandbar Sandstone|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Tanmurra Formation. Is overlain unconformably by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||
74206|Sandbar Sandstone|69673|6|Mentioned|p168 fi, p 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74206|Sandbar Sandstone|70061|5|Briefly described|Petrel Sub-basin Fig.3|Visean|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sunbird Formation.||
38068|Sea Lion Supersequence|23792|5|Briefly described|p56, Fig.D4|Kimmeridgian|Callovian|Fluvial and lacustrine clastic sediments. Equivalent to Polda Formation. Overlain by Minke supersequence. Geological Province: Bight Basin. Off shore.||||||04-MAY-05
38068|Sea Lion Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Polda Formation Equivalent.||||||
38068|Sea Lion Supersequence|61544|6|Mentioned|p367 Fig.3. |Kimmeridgian|Callovian|Ceduna Sub-basin. Syn-rift mechanical extension. ||||Is overlain by Minke Supersequence.||
38068|Sea Lion Supersequence|66578|6|Mentioned|p1007 Fig.3.|Late Jurassic|Jurassic|Ceduna Sub-Basin, Bight Basin.||||Is overlain by Minke Supersequence.||
38068|Sea Lion Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Kimmeridgian|Oxfordian|Eyre, Ceduna and Duntroon Sub-basins. Shale facies within this sequence have the best potential to be seal rocks in the Eyre Sub-basin. Good faulting seal capacity for hydrocarbons. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61.||||Overlain by the Minke Supersequence. |Sandstone, siltstone and claystone. |
38068|Sea Lion Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Kimmeridgian|Oxfordian|Bight Basin. The lithologies are unknown, not having been penetrated by wells.||||Is overlain by Minke Supersequence.||
73297|Sherbrook Supersequence|63134|2|Defined|108-110|||||||||
73297|Sherbrook Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|69297|5|Briefly described|p78, p80, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Coastal plain, deltaic and marine sediments up to 5km thick. ||||||
73297|Sherbrook Supersequence|69651|5|Briefly described|p2, p10, p12, p15, p17-21, p23, p27|Late Cretaceous|Late Cretaceous|See also p31-33, p36-40, p42-43, p45-47, p49-50. Otway Basin. Campanian to Maastrichtian age. Marginal marine to fluvial deltaic (regional regression) sediments. About 900m thick. Good oil and gas potential in the Strahan Sub-basin. An excellent offshore regional seal.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Coarse-grained sandstone, breccia-conglomerate sandy shale, sandy claystone and clayey sandstone.|
73297|Sherbrook Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9|Late Cretaceous|Late Cretaceous|Otway Basin. Up to 5km thick, basinward-thickening progradational succession of coastal plain, deltaic and marine sediments.||||||
73297|Sherbrook Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73297|Sherbrook Supersequence|70193|5|Briefly described|p283, p284 Fig 2|Thanetian|Albian|Geological province: Otway Basin. See also Sherbrook Group.|||Includes the Paaratte Formation.|||
73297|Sherbrook Supersequence|70880|5|Briefly described|p77, 83, 85|Maastrichtian|Campanian|Otway Basin.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.|Major deltaic deposition.|
73297|Sherbrook Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Late Cretaceous|Late Cretaceous|Otway Basin. Deltaic deposits thicken southwards.||||Overlies Shipwreck Supersequence. Is overlain by Wangerrip Supersequence.||
73296|Shipwreck Supersequence|63134|2|Defined|104-108|||||||||
73296|Shipwreck Supersequence|63269|5|Briefly described|p605, p607, p609|Late Cretaceous|Late Cretaceous|Otway Basin.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|69297|6|Mentioned|p78, p81, p83, p98, p110, p114-p116|Late Cretaceous|Late Cretaceous|Otway Basin. Fluvio-lacustrine, deltaic and marine sediments. |||Includes the Waarre and Flaxman Formations. |||
73296|Shipwreck Supersequence|69651|5|Briefly described|p2, p10, p12-19, p23, p26, p31-34,p36-40|Late Cretaceous|Late Cretaceous|See also p42-47, p49-50. Otway Basin. Turonian to Santonian age. Includes the economically important reservoirs of the Waarre and Flaxman Formations, and Thylacine Member (Belfast Mudstone). Over 1300m thick (at least locally). Fluvial to deltaic and marginal marine facies. An excellent offshore regional seal. Modelling diagrams.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.|Basal conglomerate; interbedded sandstone, siltstone and claystone.|
73296|Shipwreck Supersequence|70077|5|Briefly described|Nelson: p1. Regional: Fig.4; p4-7, p9-10|Late Cretaceous|Late Cretaceous|Otway Basin. Includes Sherbrook Group (Waarre and Flaxman Formations). Fluvio-lacustrine, deltaic and marine sediments. Sealed by Belfast Mudstone.||||||
73296|Shipwreck Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4, p6|Late Cretaceous|Late Cretaceous|Hosts part of Austral 3 petroleum system. Fluvio-deltaic to marine environments.||||Overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|70880|5|Briefly described|p76-78, 81-82|Santonian|Turonian|Otway Basin. Comprises three seismically-defined stratal units (described).||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
73296|Shipwreck Supersequence|71266|5|Briefly described|p614 Fig.3|Late Cretaceous|Late Cretaceous|Otway Basin. Thickens southwards.||||Unconformably overlies Eumeralla Supersequence. Is overlain by Sherbrook Supersequence.||
80798|South Perth Sequence 1|71958|4|Described|p48, p51, p54, p62, p64-p65, p67, p79|Valanginian|Valanginian|Vlaming Sub-basin. This unit is named for the South Perth Shale. A type locality is only described as "offshore, not penetrated by any wells."  Lithology is unknown but "thought to contain siliciclastics and some volcanics and volcaniclastics." On the basis of 2D seismic work is thought to be approximately 340m thick. Interpreted to have been deposited in a fluvio-deltaic to deep marine environment.||South Perth Supersequence||Conformably overlain by South Perth Sequence 2.||
80799|South Perth Sequence 2|71958|2|Defined|p51, p54-p56, p62|Hauterivian|Valanginian|Vlaming Sub-basin. This unit is named for the South Perth Shale. This sequence comrpises the Gage Sandstone, South Perth Shale and in places, the Leederville Formation. The type locality occurs in Charlotte 1 (-31.808795, 115.450375) in the interval between 1574.4 and 766 m (total thickness of 808.4m). Thickness in wells ranges from 0 to 827.1m (Mullaloo 1) and is penetrated by all wells in the study area except for Roe 1. Age determined by the presence of diagnostic microsfossils including G. mutabilis, K. scrutillinum, P. lowryi and A. alata Dinocyst zones. Deposited as two major deltaic successions in a restricted marine environment. See also p64-p65, p67-p69, p71, p79.||South Perth Supersequence|Includes the Gage Lowstand Fan.|Conformably overlies the South Perth Sequence 1 and the Parmelia Group (conformably to angular). Overlain conformably by the South Perth Sequence 3.|Fine-grained to granular feldspathic sandstone interbedded with micaceous mudstone and siltstone overlain by an argillaceous micaceous mudstone interbedded with carbonaceous, argillaceous and micaceous siltstone grading to sandstone.|
80800|South Perth Sequence 3|71958|2|Defined|p51, p55-p56, p59-60, p62, p64-p65, p80|Hauterivian|Hauterivian|Vlaming Sub-basin. Named for the South Perth Shale and Supersequence. The type locality is found in Marri 1 (-31.744767, 115.356875) in the interval between 777.2 and 548.5m (total thickness of 228.7m). Age is derived from the presence of diagnostic microfossils including A. alata and B. Jaegeri Dinocysts. In the southern Vlaming Sub-basin it ranges from predominantly mudstone with trace glauconite and pyrite with minor interbeds or glauconitic, pyritic sandstone to fine-grained glauconitic and pyritic siltstone. This unit is penetrated in all analysed wells  [this volume] and ranges in thickness between 20 to 616.2m. Deposited in environments ranging from pro-delta, shelfal, proximal delta front to fluvio-deltaic.||South Perth Supersequence||Conformably overlies the South Perth Sequence 2. Conformably overlain by the Leederville Supersequence.|Dominantly coarse-grained quartzose sandstone with trace pyrite, mica and glauconite interbedded by thin carbonaceous material with rare coal and siltstone.|
80792|South Perth Supersequence|71958|2|Defined|p38, p40-p41, p45-p46|Hauterivian|Valanginian|Vlaming Sub-basin. The name is derived from the South Perth Shale which is included in this sequence. The type locality is defined in Warnbro 1 (-32.23769, 115.347327) between 1489 and 2117.8m (a total thickness of 628.8m). Spring and Newell (1993) conducted a sequence stratigraphic analysis that found this unit coincides with four depositional sequences. Sequence stratigraphy. Age derived from the presence of diagnostic microfossils assigned to G. mutabilis, K. scrutillinum, P. lowryi, A. alata and B. Jageri. This unit is thickest in the Rottnest Trough, the northern extension of the Peel Arch and the northern Mandurah Terrace. The supersequence is absent where it onlaps the Roe High to the west, the Mandurah Terrace to the east and the Vasse Shelf and Sugarloaf Arch to the south. The maximum drilled thickness was 1326.8m intersected in Mallaloo 1. Deposited as two deltaic successions with some lava flows. See also p49, p51, p53-p56, p60-p61, p67, p77-p78, p87.||Warnbro Megasequence|Includes the South Perth Sequence 1, South Perth Sequence 2 and South Perth Sequence 3.|Overlies the Parmelia Group. Unconformably overlies the Charlotte Supersequence. Overlain by the Leederville Supersequence.|Fine-grained to very coarse feldspathic sandstone with interbedded mudstone and siltstone that is overlain by black argillaceous, micaceous mudstone that grades upwards to siltstone with minor sandstone interbeds.|
38066|Southern Right Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Neptune Formation.||||||
38066|Southern Right Supersequence|61544|6|Mentioned|p367 Fig.3. |Berriasian|Berriasian|Ceduna Sub-basin. Post-rift slow thermal subsidence.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
38066|Southern Right Supersequence|66578|6|Mentioned|p1007 Fig.3.|Early Cretaceous|Early Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
38066|Southern Right Supersequence|69297|5|Briefly described|p14 fig 2.4, p23, p25 fig 2.9|Valanginian|Berriasian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in lacustrine and fluvial environments. Basal sands of this sequence display high measured porosity and permeability and are thus good potential reservoirs for petroleum. Contains potential source rocks within lacustrine shales and coaly deposits. See also p26 fig 2.11, p27, p28, p37, p42, p45 fig 2.17, p58, p60, p61. ||||Overlies the Minke Supersequence. Overlain by the Bronze Whaler Supersequence. |Interbedded claystone, siltstone, snadstone and coal. |
38066|Southern Right Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2|Valanginian|Berriasian|Bight Basin. Copmprises Neptune Formation and topmost Echidna Formation.||||Overlies Minke Supersequence. Is overlain by Bronze Whaler Supersequence.||
17316|Steels Point Basalt|31571|2|Defined|p244|Pliocene|Pliocene|||||||
17316|Steels Point Basalt|61942|5|Briefly described|p244-246|Pliocene|Pliocene|Norfolk Island. Disconformably overlies: Cascade Basalt. Nonfragmental lenticular flows and tabular flows. Tuff at base. Thickness: 90m+. Disconformably overlies: Ball Bay Basalt. Age: 2.33-2.39 +/- 0.05My. Dated by K/Ar and palaeomagnetism.||||||27-JAN-11
74207|Sunbird Formation|61542|4|Described|p276, p277 Fig. 2, p285-6||Visean|Top unit of Weaber Group - forms part of revision by authors.Unconformably overlies Sandbar Sandstone and Tanmurra Fm. Geol. Province: Bonapart Basin/Petrel-Sub-basin. Detailed lithology included. type section described. 638-725 m in Bonaparte-1, onshore WA. Reference section in Sunbird-1, offshore NT.||||Unconformable on Tanmurra Fm. Nature of contact with underlying Sandbar Sst unknown.||26-NOV-18
74207|Sunbird Formation|67354|5|Briefly described|p73. |||||Unit in Weaber Group.||Is overlain by Wadeye Sub-Group.||
74207|Sunbird Formation|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Sandbar Sandstone and Tanmurra Formation.||12-JUL-16
74207|Sunbird Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||
74207|Sunbird Formation|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74207|Sunbird Formation|70061|5|Briefly described|Petrel Sub-basin Fig.3|Serpukhovian|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||12-JUL-16
74207|Sunbird Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sandbar Sandstone.||
38061|Tiger Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Wigunda Formation.||||||
38061|Tiger Supersequence|61544|6|Mentioned|p367 Fig.3. |Santonian|Turonian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies White Pointer Supersequence. Is overlain by Hammerhead Supersequence.||
38061|Tiger Supersequence|66578|6|Mentioned|pp1006-1007, p1010.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies White Pointer Supersequence. Is overlain by Hammerhead Supersequence.||
38061|Tiger Supersequence|69297|5|Briefly described|p14 fig 2.4, p23|Santonian|Turonian|Eyre, Ceduna and Duntroon Sub-basins. Maximum thickness fo approximately 4500m. Good potential oil and gas source rocks confirmed by dredging. See also p25 fig 2.9, p41, p44-p46, p48, p58, p60.||||Overlies the White Pointer Supersequence. Unconformably overlain by the Wobbegong Supersequence. ||
38061|Tiger Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2-3|Santonian|Turonian|Bight Basin. Comprises Wigunda Formation. Marine shales are potential source rocks and form a regional seal. Deltaic and shallow marine sandstones are potential oil and gas reservoirs according to petroleum systems modelling.||||Overlies White Pointer Supersequence. Is overlain by Tiger Supersequence.|Marginal marine, deltaic and open marine sediments thickening markedly to the south.|
18718|Turnstone Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p223|Late Cretaceous|Late Creatceous|Mory (1988). In figure, Fm = Formation. Geological Province: Bonaparte Basin. Calcareous claystones and calciluties.  Also on p228 Fig. 18.||||||01-MAR-10
18718|Turnstone Formation|13194|4|Described|p384 Tb. 4-16, p396 fig 4-60|Maastrichtian|Campanian|150-200m thick, open marine shelf deposits, fossiliferous. Only in east Ashmore Platform. Type section: Turnstone 1 well (925-1120m).||Bathurst Island Group||Overlies Vee Formation (conformably but diachronous). Grades laterally into Puffin Formation. Equivalent to upper Wangarlu Formation. |Calcareous claystone; minor marl.|
18718|Turnstone Formation|24218|5|Briefly described|p853 Fig. 5|Late Cretaceous|Late Cretaceous|Geological Province: Bonaparte Basin.||||||
18718|Turnstone Formation|41532|2|Defined|p308|Late Cretaceous||||||||
18718|Turnstone Formation|42442|2|Defined|p29|Maastrichtian|Campanian|Variation of Turnstone formation, WA. Age Late Cretaceous (Campanian to Maastrichtian).||||||01-SEP-14
18718|Turnstone Formation|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
18718|Turnstone Formation|43739|6|Mentioned|Fig.5,p38||Late Cretaceous|||||||
18718|Turnstone Formation|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
18718|Turnstone Formation|60385|5|Briefly described|p270, p272 Fig 3|Maastrichtian|Campanian|Browse Basin. |||Includes Prudhoe Member, Puffin Member, Puffin Sandstone Member, Borde Marl Member||Mudstone, with sandstone and hemipelagic marl members.|
18718|Turnstone Formation|61548|6|Mentioned|p480 Fig.3|Maastrichtian|Campanian|Northern Bonaparte Basin.||||||
18718|Turnstone Formation|62837|5|Briefly described|Stratigraphic columns|Paleocene|Late Cretaceous|Age: ~77-~65Ma. Geological Province: Northern Bonaparte Basin.||||||01-MAR-10
18718|Turnstone Formation|64695|5|Briefly described|p262 Fig.8 |Late Cretaceous|Late Cretaceous|Northern Bonaparte Basin.||||Overlies Fenelon Formation. Is overlain by Johnson Formation. ||
18718|Turnstone Formation|68223|6|Mentioned|p178 Fig.3|Maastrichtian|Campanian|||||||
18718|Turnstone Formation|69452|6|Mentioned|p36:15|||Bonaparte Basin.||Bathurst Island Group.||||12-JUL-16
18718|Turnstone Formation|70061|5|Briefly described|Regional geology; Figs.6-7|Maastrichtian|Campanian|See also Sahul: Fig.2, p2. Vulcan: Fig.2.||Bathurst Island Group.||Overlies Fenelon Formation. Is overlain by Johnson Formation.||12-JUL-16
73298|Wangerrip Supersequence|63134|2|Defined|110-111|||||||||
73298|Wangerrip Supersequence|63269|5|Briefly described|p605|Eocene|Late Cretaceous|Otway Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|69297|6|Mentioned|p79, p80, p110, p115|||||||||
73298|Wangerrip Supersequence|69651|5|Briefly described|p6,p10, p12-15, p17-23, p28, p33, p39-40|Eocene|Late Cretaceous|See also p42-47, p49-50. Maastrichtian to early Eocene age. Forms the base of the Australia-Antarctica post-breakup succession. Shallow-marine, marginal marine and deltaic deposits. Generally less than 500m thick; locally up to 1,534m. Modelling diagrams.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.|Sandstone and siltstone.|17-JUN-20
73298|Wangerrip Supersequence|70077|6|Mentioned|Regional: p4-5|Cenozoic|Cenozoic|Otway Basin.||||||
73298|Wangerrip Supersequence|70078|5|Briefly described|Regional: Fig.4; p3-4|Eocene|Paleocene|Sandstones of this unit are likely reservoirs in the Sorell Basin.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|70880|6|Mentioned|p77|Eocene|Paleocene|Otway Basin. Post-rift sedimentation; coastal plain, deltaic and inner-shelf settings.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
73298|Wangerrip Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Eocene|Paleocene|Otway Basin. Latest Maastrichtian to midddle Eocene.||||Overlies Sherbrook Supersequence. Is overlain by Nirranda Supersequence.||
80795|Warnbro Megasequence|71958|5|Briefly described|p40-p41, p45-p46, p51, p61|Aptian|Valanginian|Vlaming Sub-basin. Sequence stratigraphy. Major deltaic to shallow marine succession. Intersected in all wells from the Sub-basin.|||Includes the South Perth Supersequence and the Leederville Supersequence.|||
73301|Whalers Bluff Supersequence|63134|2|Defined|112|||||||||
73301|Whalers Bluff Supersequence|63269|5|Briefly described|p605|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|69297|6|Mentioned|p80, p98, p110, p111|||||||||
73301|Whalers Bluff Supersequence|69651|5|Briefly described|p10, p12-15, p17-19, p22, p29, p49-50|Pleistocene|Pliocene|Open marine deposits. Possible seals.||||Overlies Heytesbury Supersequence.|Calcareous claystone overlain by marls, calcarenite and calcilutite; shaly limestone overlain by calcarenite and calcilutite; quartz sandstone overlain by silty mudstone, and limestone.|
73301|Whalers Bluff Supersequence|70077|5|Briefly described|Regional: Fig.4; p4|Holocene|Miocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|70078|5|Briefly described|Regional: Fig.4; p3|Holocene|Neogene|||||Overlies Heytesbury Supersequence.|Shelfal marls and limestones.|
73301|Whalers Bluff Supersequence|70880|6|Mentioned|p77|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
73301|Whalers Bluff Supersequence|71266|5|Briefly described|p614 Fig.3, p615|Pleistocene|Pliocene|Otway Basin.||||Overlies Heytesbury Supersequence.||
38062|White Pointer Supersequence|24336|5|Briefly described|p99 Fig.3|||Correlated to the Platypus Formation.||||||
38062|White Pointer Supersequence|61544|6|Mentioned|p367 Fig.3. |Cenomanian|Cenomanian|Ceduna Sub-basin. Accelerated subsidence.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.||
38062|White Pointer Supersequence|66578|6|Mentioned|p1007 Fig.3.|Late Cretaceous|Late Cretaceous|Ceduna Sub-Basin, Bight Basin.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.||
38062|White Pointer Supersequence|69297|5|Briefly described|p14 fig 2.4, p23|Cenomanian|Cenomanian|Eyre, Ceduna and Duntroon Sub-basins. Deposited in marine to deltaic environments. Good faulting seal capacity for hydrocarbons and good potential oil and gas source rocks. Seismic interpretation suggests this unit contains a broad band of coaly sediments. Maximum thickness of approximately 5000m. See also p25 fig 2.9, p26 fig 2.11, p28, p37, p41-p44, p45 fig 2.17, p58, p60.||||Overlies the Blue Whale Supersequence. Overlain by the Tiger Supersequence. ||
38062|White Pointer Supersequence|70067|5|Briefly described|Ceduna: Fig.2; p2. Regional: Fig.2; p2|Cenomanian|Cenomanian|Bight Basin. Consists mostly of Platypus Formation. Potential reservoir. Coals are potential source rocks.||||Overlies Blue Whale Supersequence. Is overlain by Tiger Supersequence.|Prograding deltaic sediments, including a broad band of coaly sediments.|
38054|Wobbegong Supersequence|24336|2|Defined|p99 Fig.3|Ypresian||Correlated to Pidinga Formation.||||||
38054|Wobbegong Supersequence|61544|6|Mentioned|p367 Fig.3. |Eocene|Eocene|Ceduna Sub-basin. Post-break-up thermal subsidence.||||Is overlain by Dugong Supersequence.||
38054|Wobbegong Supersequence|66578|6|Mentioned|pp1006-1007, p1010.|Paleogene|Paleogene|Ceduna Sub-Basin, Bight Basin.||||Unconformably overlies Hammerhead Supersequence. Is overlain by Dugong Supersequence.||
38054|Wobbegong Supersequence|69297|6|Mentioned|p14 fig 2.4, p25 fig 2.9|Ypresian|Thanetian|Eyre, Ceduna and Duntroon Sub-basins. See also p26 fig 2.11, p28, p58, p60, p61, p64. ||||Unconformably overlies the Tiger Supersequence. Overlain by the Dugong Supersequence. ||
38054|Wobbegong Supersequence|70067|5|Briefly described|Ceduna: Fig.2. Regional: Fig.2; p4-5|Ypresian|Thanetian|Bight Basin. Comprises Pidinga Formation. Sealed by thick transgressive marls of basal Dugong Supersequence.||||Overlies Hammerhead Supersequence. Is overlain by Dugong Supersequence.||
