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RB 59/00049 SADM Fortville 003 well completion report.
Fortville No. 3 was drilled as a combined water and stratigraphic well. The sequence which was encountered consists of 62 feet recent sediments; 338 feet Lower Tertiary sands and lignitic clays; 2605 feet Cretaceous sediments and 483 feet Mooga...-
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Published: 01 Jan 1967
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RB 59/00115 Micropalaeontology of bores at Fortville (appendix C).
To a total depth of 3610 feet Fortville No. 3 well intersected 62 feet of recent sand, 368 feet of Tertiary sand, silt and clay, 887 feet of Canomanian (Winton Series, Blanchewater Formation in part at least) sandstones, siltstones and dolomite; 1243...-
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Published: 01 Jan 1967
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RB 80/00116 Mesozoic stratigraphy of the Frome Embayment.
This study covers a southern lobe of the Eromanga Basin known as the Frome Embayment, which extends W-E from the Flinders Ranges to the Barrier Ranges, and southwards from the vicinity of Moolowatana Station to the Scott Hill-Mundaerno Hill region....-
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Published: 01 Feb 1980
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RB 79/00015 Early Cretaceous palynology of SADME Coongra 1, southwestern Eromanga Basin.
Coongra 1 stratigraphic well, located at Latitude 27º 8´ 15"S, Longitude 134º 8´ 20"E was drilled to 200.20 m total depth in Cretaceous sediments of the south-western Eromanga Basin, in an area of shallow basement. Two drill cuttings samples taken...-
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Published: 01 Jan 1979
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RB 78/00086 Andamooka Opalfields. A geological guide for the opal prospector.
During May - September 1978, 66 shafts were sunk under subsidised mining programmes to encourage testing of new areas. The new fields of Stans Hill and Yarloo West were established subsequent to the discovery of opal in Shafts 17 and 49.-
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Published: 01 Jan 1978
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Hydrocarbon potential of the Jurassic and Lower Cretaceous sediments from five wells in the Eromanga Basin, South Australia.
Organic matter in Jurassic and lower Cretaceous sediments from 5 wells in the central Eromanga Basin was studied microscopically. The lower Jurassic Birkhead Formation, upper Jurassic to lower Cretaceous Murta Member and lower Cretaceous Transition...-
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Hydrocarbon potential and environmental interpretations of the Jurassic - Lower Cretaceous section in five wells in the Eromanga Basin.
Five wells along a north-south trending section in the southern Eromanga Basin were studied using petrographic techniques to delineate petroleum source rocks and possibly aid in environmental interpretation. The dispersed organic matter (d.o.m.) in...-
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RI 029 S.A.G. Fortville No. 3 Well Completion Report
There is no abstract created for this record-
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RB 00658 Delhi-Frome-Santos Betoota 001 well. Subsurface stratigraphy and micropalaeontological study.
Betoota No. 1 Well was drilled to a depth of 9824 feet and penetrated a sedimentary sequence of Cretaceous and Jurassic rocks to 5757 feet before entering steeply dipping red bed conglomerate and sandstone the age of which is uncertain. Marine...-
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Published: 01 Jun 1960
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RB 00719 Explanatory Notes for a structural contour map of portion of the Great Artesian Basin, revised September 1964.
The structural contour map compiled in 1963 for the South Australian portion of the Great Artesian Basin has been revised with information available up to September, 1964. The Transition Beds and equivalents are used as the structural datum formation,...-
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Published: 01 Aug 1900
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RB 2009/00001 Explanatory Notes for [the] CALLABONNA 1:250 000 Geological Map, sheet SH 54-6.
The CALLABONNA map area includes the southern end of the Strzelecki Desert and the north- eastern Flinders Ranges, between latitudes 29° to 30° S and longitudes 139° 30' to 141° E. Cameron Corner adjoins New South Wales and Queensland in the...-
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Published: 01 Oct 2009
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ExpNotes CALLABONNA: Explanatory Notes CALLABONNA, SH 54-06.
There is no abstract created for this record.-
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ExpNotes STRZELECKI: Explanatory Notes STRZELECKI, SH 54-02.
The STRZELECKI 1:250 000 map area lies adjacent to the NSW border in the centre of the Strzelecki Desert, and covers some of the main hydrocarbon producing areas in SA around Moomba. Most of these oil and gas fields are located in the northern half of...-
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