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Oil Prospecting Licence 4, Lake Cootabarlow area. Progress reports to licence full surrender, for the period 18/11/1948 to 9/1/1950, plus technical correspondence and results of drill sample analyses, as later submitted to the SA Department of Mines.
A 50 square mile area centred immediately south-southeast of Lake Cootabarlow, and lying ~12 miles south of the Moolawatana 1 water bore, was taken up by Australian - based holding company Frome - Broken Hill Co. Pty Ltd as an Oil Prospecting Licence...-
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Source rock and petroleum geochemistry of the Pedirka Basin, Simpson Desert Basin and superjacent Eromanga Basin.
Report collates in tabular format the available MESA open file, published literature-based and other University of Adelaide organic geochemical data on the hydrocarbon prospectivity of sediments underlying the Simpson Desert region. Likely oil...-
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Purni 1. Test reports.
Contains results of government consultants' palynological and palaeontological studies of drill cuttings and cores, plus data obtained from DST fluid sample water and gas analyses and from conventional core analyses and source rock analytical...-
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MESA Pedirka and Eromanga Basins Thermal and Tectonic History Project. Reports for the period January 1995 to December 1996.
Apatite fission track analysis (AFTA), detailed source rock property and organic maceral vitrinite reflectance data has been collected from several key wells neighbouring the Eringa Trough, as part of a collaborative ARC grant project run by MESA and...-
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Thermal history reconstruction in Cooper-Eromanga Basin wells using apatite and zircon fission track analysis and vitrinite reflectance.
Results of a study aimed at providing a better thermal history framework for understanding the post-Palaeozoic thermal evolution of parts of the Cooper-Eromanga Basin, South Australia, based on apatite fission track analysis, zircon fission track...-
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Cretaceous stratigraphy of the southwestern Eromanga Basin - Part 1: general introduction, formation tops and log correlation diagrams for the interval Toolachee Formation to 'C'-Horizon.
This company study of the Eromanga Basin sequence within PELs 5 and 6 and ATP 259P was designed to provide the Delhi Petroleum exploration consortium with data on the following: (a) thickness and correlation of Aptian-Albian units throughout the...-
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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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RI 028 The Geology of the Marree 1:250,000 Map Area
There is no abstract created for this record-
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RB 00655 Delhi-Frome-Santos Innamincka no. 1 well. Subsurface stratigraphy and micropalaeontological study. Final report.
Innamincka no. 1 well was drilled to a depth of 12,638 feet KB and penetrated a sedimentary sequence of Mesozoic and Palaeozoic rocks ranging in age from Cretaceous to ?Devonian. Marine Cretaceous (Albian) carbonaceous mudstones and siltstones were...-
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Published: 08 Feb 1960
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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 00839 Post-Cretaceous structure of the Cooper Basin region in SA, and its relevance to petroleum migration and entrapment.
The Cooper Basin region has had a long structural history, reflected in differing structural styles ranging from thrust faults, to extensional horst and graben developments, to wrenching. The timing of this structuring in relation to the main period...-
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RB 00753 Kalladeina bore - Lithological sequence, surface to 1 210 feet.
The near surface section encountered in Kalladeina 1 contains a thick Plio-Pleistocene section, whilst the Lower Tertiary sediments ubiquitously present in the Cooper's Creek Basin, are either absent or very thin. Of particular interest is the...-
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Published: 01 Aug 1900
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RB 00679 Delhi-Santos' Dullingari 1 subsurface stratigraphy and micropalaeontological study. Progress report.
Dullingari 1 to a depth of 2798 metres has intersected a sedimentary sequence of Tertiary, Mesozoic and Permian rocks, the age of the sediments below 2756 metres being at present uncertain. This report presents lithological data and stratigraphic...-
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Published: 01 Aug 1900
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ExpNotes CURDIMURKA: Explanatory Notes CURDIMURKA
There is no abstract created for this record-
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ExpNotes POOLOWANNA: Explanatory Notes POOLOWANNA
There is no abstract created for this record-
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Bull 040 Cretaceous Biostratigraphy of the Great Artesian Basin in South Australia
After its formation as a single sedimentary entity the Great Artesian Basin provided a marine environment only during the Cretaceous Aptian, Albian and early Cenomanian in South Australia. Santos' Oodnadatta 1 well (1957), continuously cored through...-
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RB 70/00100 Reconnaissance survey and photo-geological interpretation Gason Dome area of the Great Australian Artesian Basin, South Australia.
The GASON 1:250,000 map area is located in the northeast of South Australia, on the Birdsville Track. The map area includes the Gason, Dome, a topographically low structure with a northeasterly trending axis, and shallow dips on its flanks. The Upper...-
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Published: 24 Jul 1970
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RB 71/00142 Upper Cretaceous palynology of the Winton Formation, GASON 1:250 000 sheet.
Cores yielded well preserved and diverse microflora of the Tricolpites pannosus zone of Albian (?) Cenomanian age. Core from Gason 2 reflects restricted, possibly swamp, environment, whereas the other cores represent lacustrine sedimentation. Recycled...-
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Published: 06 Sep 1971
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RB 73/00096 Explanatory Notes for the GASON 1:250 000 geological map.
The Gason 1:250 000 sheet area is centred about 850 km north of Adelaide, in the South Australian portion of the Great Artesian Basin. The area mapped includes most of the Gason Dome, a gentle upwarp in a relatively flat-lying sequence of Mesozoic and...-
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Published: 12 Apr 1973
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RB 73/00026 Measured sections from the INNAMINCKA 1:250 000 area.
There is no abstract created for this record-
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Published: 31 Jan 1973
