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
83165|Barrow Group, Upper|69689|5|Briefly described|p16|Cretaceous|Cretaceous|Exmouth Sub-basin, Northern Carnarvon Basin. Part of regional play interval K20.|||or lateral equivalents? Mardie Greensand: Birdrong, Zeepaard Formations.|Overlies Lower Barrow Group. Is overlain by Muderong Shale.||05-APR-22
79321|Blacktip member|69452|6|Mentioned|p36:18-19|||Gorter et al. (2008), for the glacigenic top of the Kuriyippi Formation, which they argue should be assigned to the younger Treachery Formation. [This is an unfortunate misquote, as Gorter et al. in fact capitalised the name: Blacktip Member]. Forms a petroleum reservoir in Blacktip-1.||||||12-JUL-16
68853|Blue Whale supersequence|23792|5|Briefly described|p56, Fig.D4|Cenomanian|Albian|Equivalent to Ceduna Formation. Marine shales. Overlies Bronze Whaler supersequence. Overlain by White Pointer supersequence. Geological Province: Bight Basin. Off shore.||||||04-MAY-05
68850|Bronze Whaler supersequence|23792|5|Briefly described|p56, Fig.D4|Albian|Valanginian|Equivalent to Upper and Lower Borda Formation. Overlies Southern Right supersequence. Overlain by Blue Whale supersequence. Fluvio-lacustrine to marine sediments. Geological Province: Bight Basin. Off shore.||||||
34378|Cooper Cliff Formation|22682|6|Mentioned|p30|||Huronian Supergroup||||||
83166|Cossigny Limestone|69689|6|Mentioned|p16|Triassic|Triassic|Exmouth, Barrow, Dampier and Beagle Sub-basins, Northern Carnarvon Basin, Roebuck Basin. Appears as Cossigny Lst. Part of regional Play interval TR10.||||||05-APR-22
83167|Dingo Claystone, Lower|69689|6|Mentioned|p16|Jurassic|Jurassic|Exmouth, Barrow Sub-basins, Northern Carnarvon Basin. Also misspelt as Dino Clyst. Part of regional play interval J40.||||Overlies Eliassen Formation.||05-APR-22
83168|Dingo Claystone, Upper|69689|6|Mentioned|p16|Jurassic|Jurassic|Barrow Sub-basin, Northern Carnarvon Basin. Part of regional play interval J50.||||Overlies Lower Dingo Claystone.||05-APR-22
68858|Dugong supersequence|23792|5|Briefly described|p56, Fig.D4|Recent|Early Eocene|Informal - see Dugong Supersequence. Equivalent to Wilsons Bluff Limestone and Nullabor Limestone. Overlies the Wobbegong supersequence. Open marine shelf carbonates. See also Dugong Supersequence. Geological Province: Bight Basin. Off shore.||||||15-JUN-05
34380|Elliot Lake Group|22682|5|Briefly described|p30||Siderian|2450 Ma. Huronian Supergroup. Canada.||||||03-MAR-10
79738|Elm Sandstone|70934|5|Briefly described|unpaginated|Oxfordian|Oxfordian|Swan Graben, Vulcan Sub-basin. Slope-fan unit. Occurs as separate to partially-separate fault blocks in the Vesta oil and gas field, Swan Graben. Intersected by wells Vesta-1 and Vesta-2. Prospective reservoir target.||Lower Vulcan Formation||||24-JAN-17
79258|Eucla 1|70067|5|Briefly described|Regional: Fig.3|Ypresian|Thanetian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to Wobbegong Supersequence.||
79259|Eucla 2|70067|5|Briefly described|Regional: Fig.3|Holocene|Ypresian|Bremer Sub-basin, Bight Basin. A sequence-stratigraphic unit of Sequence rank.||||Equivalent to Dugong Supersequence.||
6680|Fish Canyon Tuff|22678|6|Mentioned|p724|||||||||
6680|Fish Canyon Tuff|41749|6|Mentioned|p475|||||||||
77108|Flamingo Sandstone|61548|6|Mentioned|p480 Fig.3|Early Cretaceous|Late Jurassic|Northern Bonaparte Basin.||||||
77108|Flamingo Sandstone|68223|6|Mentioned|p178 Fig.3|Berriasian|Tithonian|||||||
83171|Frigate Formation, Upper|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Bonaparte Basin. Part of regional play interval K10.||||Is overlain by Echuca Shoals Formation.||05-APR-22
69957|Gregory Rift trachytes|22671|6|Mentioned|p844|||Informal name.||||||
32502|Gunflint Chert|32339|6|Mentioned|p146||Proterozoic|||||||
32502|Gunflint Chert|61732|6|Mentioned|p140|Paleoproterozoic|Paleoproterozoic|||||||07-FEB-11
7901|Gunflint Formation|40899|6|Mentioned|p25|||||||||
7901|Gunflint Formation|50222|6|Mentioned|p328|||Includes iron-formations.  Geological Province: Superior Province.||||||
7901|Gunflint Formation|66109|6|Mentioned|p195|Proterozoic|Proterozoic|Involved in the first study to document elemental organic carbon in microscopic fossils using Secondary Ion Mass Spectrometry.||||||
7902|Gunflint Iron Formation|23529|6|Mentioned|p13|||||||||
7902|Gunflint Iron Formation|32339|6|Mentioned|p147||Proterozoic|||||||
7902|Gunflint Iron Formation|41997|6|Mentioned|p78|||||||||
7902|Gunflint Iron Formation|66427|6|Mentioned|p54, |||||||||
70218|Gunflint chert|61579|5|Briefly described|p72, p77|Paleoproterozoic|Paleoproterozoic|Informal name.  Contains microfossil filament populations such as Gunflintia filaments. Age: 1900Ma. ||||||07-NOV-08
70218|Gunflint chert|67668|6|Mentioned|p.162. ||Orosirian|Contains bona fide microfossils (De Gregorio et al. 2009).|c.1900 Ma.|||||
68856|Hammerhead supersequence|23792|5|Briefly described|p56, Fig. D4|Maastrichtian|Santonian|Informal - see Hammerhead Supersequence. Equiv. to Potoroo Fm. Shelf margin delta complexes. Overlies Tiger supersequence. Overlain unconformably by Wobbegong supersequence.  Geological Province: Bight Basin. Offshore. See also Hammerhead Supersequence.||||||15-JUN-05
79268|Heywood Formation, Lower|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Albian|Barremian|See also Northern: Fig.2. Yampi: Fig.2. Yampi and Leveque Shelves, Browse Basin.||Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Upper Heywood Formation. Equivalent to Lower Jamieson Formation.||12-JUL-16
79269|Heywood Formation, Upper|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Turonian|Albian|See also Northern: Fig.2. Yampi: Fig.2. Yampi and Leveque Shelves, Browse Basin.||Bathurst Island Group.||Overlies Lower Heywood Formation. Is overlain by Puffin Formation. Equivalent to Upper Jamieson Formation.||12-JUL-16
34379|Huronian Supergroup|22682|6|Mentioned|p30|||||||||
79266|Ichthys Formation|70064|6|Mentioned|Regional p6, p8. Northern: p2|Callovian|Callovian|After Ban and Pitt (2006). Presumably named after the Ichthys gas accumulation. Apparently subsumed into the Montara Formation: "reported as the Ichthys Formation, but included within the Montara Formation". Appears in Northern: p2 as Montara (Ichthys) Formation.||||||12-JUL-16
77109|Iris Marl|60386|6|Mentioned|p302|Kimmeridgian|Kimmeridgian|Browse Basin/Bonaparte Basin. Limestone nearshore-shelf.||||||
77109|Iris Marl|61548|6|Mentioned|p480 Fig.3|Kimmeridgian|Kimmeridgian|Northern Bonaparte Basin.||||||
77109|Iris Marl|68223|6|Mentioned|p178 Fig.3, p180 Fig.5|Kimmeridgian|Kimmeridgian|||||||
28621|Jamieson Formation, Lower|42053|5|Briefly described|Fig.2 p29|||||||||21-OCT-15
28621|Jamieson Formation, Lower|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
28621|Jamieson Formation, Lower|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Informal - see Jamieson Formation. Age: ~114-~106Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||09-NOV-06
28621|Jamieson Formation, Lower|69297|5|Briefly described|p305|Albian|Aptian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Bathurst Island Group||Overlies the Echuca Shoals Formation. Overlain by the Upper Jamieson Formation. |Mudstones or shales.|
28621|Jamieson Formation, Lower|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Browse, Bonaparte Basins.||||Overlies Echuca Shoals Formation.||
28621|Jamieson Formation, Lower|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Albian|Aptian|See also Northern: Fig.2; p1. Yampi: Fig.2. Browse Basin. Oil-prone, immature-marginally mature shallow marine source rocks. Gas show in Abalone 1 and Abalone Deep 1 wells. Potential reservoir.||Bathurst Island Group.||Overlies Echuca Shoals Formation. Is overlain by Upper Jamieson Formation.|Includes shallow-marine sandstones, submarine fans and ponded turbidites.|12-JUL-16
8850|Jamieson Formation, Upper|42066|5|Briefly described|Fig.3 p199|||||||||21-OCT-15
8850|Jamieson Formation, Upper|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Informal - see Jamieson Formation. Age: ~106-~95Ma. Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||01-MAR-10
8850|Jamieson Formation, Upper|69297|5|Briefly described|p305|Cenomanian|Albian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Bathurst Island Group||Overlies the Lower Jamiesone Formation. Overlain by the Woolaston Formation.|Mudstones or shales.|
8850|Jamieson Formation, Upper|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Cenomanian|Albian|See also Northern: Fig.2; p1. Yampi: Fig.2; p2. Browse Basin. Oil-prone, immature-marginally mature shallow marine source rocks. Gas show in Phrixus 1 well. Potential reservoir and regional seal.||Bathurst Island Group.||Overlies Lower Jamieson Formation. Is overlain by Wooolaston Formation.|Includes shallow-marine sandstones, submarine fans and ponded turbidites.|12-JUL-16
8854|Jamieson Member, Lower|42053|5|Briefly described|Fig.3 p30|||||||||21-OCT-15
83170|John Brookes Sandstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Barrow Sub-basin, Northern Carnarvon Basin. Part of regional play interval K20.||||||05-APR-22
79264|Macedon Formation|70066|5|Briefly described|Regional: p12|||Exmouth Sub-basin, Northern Carnarvon Basin. The Cimatti 1 well intersected a gross 15m oil column in this unit.||||||
68845|Minke supersequence|23792|5|Briefly described|p56, Fig.D4|Berriasian|Tithonian|Fluvial and lacustrine clastic sediments. Equivalent to Echigna Formation. Overlies the Sea Lion supersequence. Overlain by Southern Right supersequence. Geological Proivnce: Bight Basin. Off shore.||||||
14244|Norfolk Islands basalt|36381|6|Mentioned|p196|||||||||
35913|Phalaborwa Carbonatite|23353|5|Briefly described|310|Rhyacian|Rhyacian|~2060Ma||||||
35913|Phalaborwa Carbonatite|24535|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Age: 2060 Ma. Used as a calibration standard for dating of Glenayle Dolerite.||||||26-NOV-13
15137|Phillip Island basalt|36381|6|Mentioned|p196|||||||||
79256|Sailfish Volcanics|70076|5|Briefly described|South-Eastern: Fig.6|Langhian|Langhian|||Seaspray Group.||||
68849|Southern Right supersequence|23792|5|Briefly described|p56, Fig.D4|Berriasian|Berriasian|Equivalent to Neptune Formation. Overlies Minke supersequence. Overlain by Bronze Whaler supersequence. Fluvio-lacustrine to marine sediments. Geological Province: Bight Basin. Off shore.||||||
68855|Tiger supersequence|23792|5|Briefly described|p56, Fig.D4|Santonian|Turonian|Equivalent to Wigunda Formation. Overlies White Pointer supersequence. Overlain by Hammerhead supersequence. Open marine sediments. Off shore.||||||
18547|Transvaal Dolomite|41663|6|Mentioned|p38|||||||||14-DEC-06
42364|Vulcan Formation, Lower|5952|5|Briefly described|p217|||Informal name.||||||05-MAY-09
42364|Vulcan Formation, Lower|7142|6|Mentioned|p350 Fig.4.|Late Jurassic|Middle Jurassic|Browse Basin.||||Overlies Plover and Montara Formations. Is overlain by Upper Vulcan Formation.||
42364|Vulcan Formation, Lower|13292|5|Briefly described|pp308-311.|Late Jurassic|Late Jurassic|See Vulcan Formation. A relatively uniform shale, it is generally regarded as the main hydrocarbon source rock in the Vulcan Graben. Considerable variation in thickness lessens reliability of maturity maps.||||||
42364|Vulcan Formation, Lower|13353|6|Mentioned|p398.|Late Jurassic|Late Jurassic|Use Vulcan Formation. Includes hydrocarbon source rocks.||Unit in Swan Group.||Overlies Plover Formation.||24-JAN-17
42364|Vulcan Formation, Lower|13354|6|Mentioned|p375 Fig.6.|Late Jurassic|Middle Jurassic|Unit of Swan Group. Overlies Plover Formation of the Troughton Group, and underlies Upper Vulcan Formation.||107||||28-OCT-14
42364|Vulcan Formation, Lower|22663|5|Briefly described|AC97 1-4 Fig.4||Late Jurassic|Swan Group||||||
42364|Vulcan Formation, Lower|23378|4|Described|p180 Fig.2; p177-8, 196, 198-201|Kimmeridgian|Oxfordian|Invalid name, part of Vulcan Formation used in the same paper. Should have lower case "l". of Vulcan Sub-basin.||||||
42364|Vulcan Formation, Lower|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Informal name - see Vulcan Formation. Geological Province : Vulcan Sub-Basin||||||
42364|Vulcan Formation, Lower|24207|4|Described|p209-210|Kimmeridgian|Callovian|Geological Province: Vulcan Sub-basin.||||||
42364|Vulcan Formation, Lower|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin. Informal name||||||09-MAR-05
42364|Vulcan Formation, Lower|42053|4|Described|p40|||||||||
42364|Vulcan Formation, Lower|42066|6|Mentioned|Fig.3 p199|||||||||
42364|Vulcan Formation, Lower|42081|5|Briefly described|Fig.2 p291|||||||||
42364|Vulcan Formation, Lower|60378|4|Described|p95, 98, 104-119|Late Jurassic|Late Jurassic|Organic-rich marine succession. Petroleum source rock? Thickness variations and distribution discussed.||presumably informal subdivision of Vulcan Formation||||
42364|Vulcan Formation, Lower|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Late Jurassic|Late Jurassic|The Vulcan Formation is not formally divided into Lower and Upper units.||The Vulcan Formation (without the 'Lower') is a unit in the Swan Group.||||
42364|Vulcan Formation, Lower|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Middle Jurassic|Age: ~156-145 Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||09-NOV-06
42364|Vulcan Formation, Lower|63358|5|Briefly described|p4 Fig. 1.3|Kimmeridgian|Callovian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
42364|Vulcan Formation, Lower|64689|5|Briefly described|p7-14, p17, p19|Tithonian|Oxfordian|Valanginian. Vulcan Sub-basin. Sealing blanket from syn-rift deposition. Source for oil shows in Crux-1 from adjacent Heywood Graben.||||Unconformably overlies Plover Formation. Is overlain by Upper Vulcan Formation.|Syn-rift shale.|
42364|Vulcan Formation, Lower|64696|6|Mentioned|p125, p126, p127 Fig.2, p131|Kimmeridgian|Callovian|See also p134-138, p140. Syn-rift succession. Has important source (basal 20-30 m) and reservoir rocks.||||Overlies Plover Formation unconformably.||
42364|Vulcan Formation, Lower|64697|6|Mentioned|p84 Fig.2, p86, p88, p91-92|Late Jurassic|Late Jurassic|||||||
42364|Vulcan Formation, Lower|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Kimmeridgian|Kimmeridgian|Swan Group. Underlies the Upper Vulcan Formation, overlies the Montana Formation. Mount Ashmore Dome. Shallow marine sandstone and claystone.||||||
42364|Vulcan Formation, Lower|69689|6|Mentioned|p16|Jurassic|Jurassic|Browse, Bonaparte Basins.||||Is overlain by Upper Vulcan Formation.||
42364|Vulcan Formation, Lower|70061|5|Briefly described|Regional geology Fig.7, p9. Vulcan:Fig.2|Tithonian|Callovian|Contains mature marine, oil- and gas-prone source rocks for all the produced oils in the Vulcan Sub-basin.||Swan Group.|||Predominantly marine mudstones that contain variable amounts of terrigenous organic matter.|12-JUL-16
42364|Vulcan Formation, Lower|70064|5|Briefly described|Regional Fig. 6; p6-8. Central: Fig.2|Tithonian|Callovian|See also Northern: Fig.2; p2. Yampi: Fig.2. Browse Basin. An oil source in the Heywood Graben. Potential reservoir. Forms seals for Plover Formation reservoirs.||Swan Group.||Overlies Troughton Group. Is overlain by Upper Vulcan Formation.||12-JUL-16
42364|Vulcan Formation, Lower|70934|6|Mentioned|unpaginated|Late Jurassic|Late Jurassic|Source rocks in the Swan Graben.|||Elm Sandstone|||
42365|Vulcan Formation, Upper|7142|6|Mentioned|p350 Fig.4.|Early Cretaceous|Late Jurassic|Browse Basin.||||Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||
42365|Vulcan Formation, Upper|12466|5|Briefly described|p173.|Late Jurassic|Late Jurassic|[See Vulcan Formation]. Westralian 2 (W2) oils source rock; hydrocarbons generated from mixed terrestrial and marine organic matter in a clastic marine setting.||||||
42365|Vulcan Formation, Upper|13292|6|Mentioned|pp310-311.|Late Jurassic|Late Jurassic|See Vulcan Formation.||||||
42365|Vulcan Formation, Upper|13353|6|Mentioned|p398.|Early Cretaceous|Early Cretaceous|Use Vulcan Formation. Includes hydrocarbon source rocks.||Unit in Swan Group.||Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||
42365|Vulcan Formation, Upper|13354|6|Mentioned|p375 Fig.6, p383.|Late Jurassic|Late Jurassic|Unit of Swan Group. Overlies Lower Vulcan Formation and underlies Echuca Shoals Formation of the Bathurst Island Group. A suggested source of hydrocarbons in Gwydion 1 well, Yampi Shelf.||187||||28-OCT-14
42365|Vulcan Formation, Upper|22663|5|Briefly described|AC97 1-4 Fig.4|Early Cretaceous|Late Jurassic|Swan Group||||||
42365|Vulcan Formation, Upper|23378|4|Described|p180 Fig.2; p196|Early Cretaceous|Late Jurassic|Invalid name, part of Vulcan Formation used in the same paper. Should have lower case "u". of Vulcan Sub-basin.||||||
42365|Vulcan Formation, Upper|24171|5|Briefly described|p722 Fig. 3|Jurassic|Jurassic|Informal name - see Vulcan Formation. Geological Province : Vulcan Sub-Basin||||||
42365|Vulcan Formation, Upper|24207|4|Described|p211, p209 Fig. 5|Valanginian|Tithonian|Characterised by thick restricted marine mudrocks and coarse clastic sub-marine fan deposits near inter-graben highs.  Geological Province: Vulcan Sub-basin.||||||
42365|Vulcan Formation, Upper|24427|5|Briefly described|p49 Fig.2|Early Cretaceous|Tithonian|Geological Province: Bonaparte Basin. Informal name.||||||09-MAR-05
42365|Vulcan Formation, Upper|42053|4|Described|p40|||See also Fig.3||||||
42365|Vulcan Formation, Upper|42066|6|Mentioned|Fig.3 p199|||||||||
42365|Vulcan Formation, Upper|60378|5|Briefly described|p95, Fig 2|Early Cretaceous|Late Jurassic|Sometimes a petroleum seal.||presumably informal subdivision of Vulcan Formation||||
42365|Vulcan Formation, Upper|60634|6|Mentioned|p1167 Fig.2, p1168 Fig.3.|Early Cretaceous|Late Jurassic|The Vulcan Formation is not formally divided into Lower and Upper units.||The Vulcan Formation (without the 'Upper') is a unit in the Swan Group.||||
42365|Vulcan Formation, Upper|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Age: 145-~137Ma. Geological Province: Vulcan Sub-basin and Londonderry High.||||||
42365|Vulcan Formation, Upper|63358|5|Briefly described|p4 Fig. 1.3|Valanginian|Tithonian|See also p16 Fig. 3.1, p133 Fig. 3.71 and p172 Appendix Table A1.11.||||||01-MAR-10
42365|Vulcan Formation, Upper|64689|5|Briefly described|p7 Fig.6, p11 Fig.11, p13-15, p17-19|Valanginian|Tithonian|Valanginian. Vulcan Sub-basin. Sealing blanket from syn-rift deposition.|||||Syn-rift shale.|
42365|Vulcan Formation, Upper|64696|6|Mentioned|p127 Fig.2, p134, p135-136|Berriasian|Tithonian|A gas column in this unit, in Kalyptea-1, was sourced from the Echuca Shoals Formation.||||||
42365|Vulcan Formation, Upper|64697|6|Mentioned|p84 Fig.2, p92|Early Cretaceous|Late Jurassic|An oil pool was intersected by Cultus Petroleum's Tenacious-1 in 1997.||||||
42365|Vulcan Formation, Upper|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Berriasian|Berriasian|Swan Group. Underlies the Echuca Shoals Formation, overlies the Lower Vulcan Formation. Mount Ashmore Dome. Deep marine sandstone.||||||
42365|Vulcan Formation, Upper|69689|6|Mentioned|p16|Cretaceous|Jurassic|Browse, Bonaparte Basins.||||Overlies Lower Vulcan Formation. Is overlain by Heywood Formation.||
42365|Vulcan Formation, Upper|70061|6|Mentioned|Regional geology Fig.7. Vulcan: Fig.2|Valanginian|Tithonian|||Swan Group.||||12-JUL-16
42365|Vulcan Formation, Upper|70064|5|Briefly described|Regional Fig. 6; p6, p8. Central: Fig.2|Valanginian|Tithonian|See also Northern: Fig.2; p2. Yampi: Fig.2. Browse Basin.||Swan Group.|Brewster Member.|Overlies Lower Vulcan Formation. Is overlain by Echuca Shoals Formation.||12-JUL-16
68854|White Pointer supersequence|23792|5|Briefly described|p56, Fig.D4|Cenomanian|Cenomanian|Equivalent to Platypus Formation. Overlies Blue Whale supersequence. Overlain by Tiger supersequence. Geological Province: Bight Basin. Off shore.||||||04-MAY-05
68857|Wobbegong supersequence|23792|5|Briefly described|p56, Fig.D4|Early Eocene|Late Paleocene|Equivalent to Pidinga Formation. Transgressive sediments. Unconformably overlies Hammerhead supersequence. Overlain by Dugong Supersequence. Geological Province: Bight Basin. Off shore.||||||
