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RB 84/00001 Review of exploration activity in the Arckaringa Basin region 1858-1983. Volume 1 - Report.
State Government and exploration company data are compiled into a review of the geology and resource potential of the region. Attention is directed to the relative lack of basic lithological, petrophysical and biostratigraphic data, despite the...-
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Published: 01 Sep 1984
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RB 81/00005 Stratigraphy of the TARCOOLA 1:250 000 map sheet area.
Brief summary progress report.-
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Published: 01 Jan 1981
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RB 91/00041 Geology of the KINGOONYA 1:250 000 map sheet area.
Extensive field geological mapping, augmented by petrological and geochemical studies, reinterpretation of company drilling and water-bore logs and a nine-hole drilling programme has detailed the geology of the KINGOONYA area. The stratigraphy spans...-
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Published: 01 Apr 1991
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RB 93/00010 Explanatory Notes for the WARRINA 1:250 000 geological map.
The oldest rocks on WARRINA outcrop in the Peake and Denison Inliers, which comprise the Davenport and Denison Ranges and small inliers to the east. Basement in this area consists of Palaeoproterozoic metamorphic rocks which were intruded by...-
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Published: 01 Jun 1994
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RB 90/00014 Explanatory Notes for the TALLARINGA 1:250 000 geological map.
There is no abstract created for this record-
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Published: 01 Mar 1991
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RB 91/00052 Ruby Hill 1. Well completion report.
SADME stratigraphic drillhole Ruby Hill 1 was sited 10.4 km east of William Creek, and was designed to penetrate Early Cretaceous rocks of the Eromanga Basin and to sample pre-Mesozoic basement. It intersected 191 m of the Eromanga Basin sedimentary...-
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Published: 01 May 1991
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PACE Theme 2 (drilling partnerships with PIRSA and industry): Year 1 partnership DPY1-47 - [prospecting for] water in Permian palaeochannels draining the Mount Woods Inlier. Project final report.
Development of the Prominent Hill copper-gold deposit in the Mount Woods region will require an adequate source of water to support planned mining and ore processing operations, currently estimated to involve at least 6 million tonnes of ore per year....-
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Published: 10 Jun 1905
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Nilpinna Homestead area (part of the Australian Diamond Exploration joint venture). Progress reports and final report to licence expiry/full surrender, for the period 16/1/1980 to 22/2/1987.
Diamond exploration undertaken in the Peake and Denison Ranges included the acquisition and processing of aerial magnetic, radiometric and heliborne magnetic and VLF-EM surveys, with follow-up ground magnetic and Sirotem surveys, plus extensive...-
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Geology and hydrocarbon prospects of the Arckaringa Block.
Due to its thin sequence and shallow depth of burial, most of the Arckaringa Basin is predicted to be immature for hydrocarbon generation in traditional terms. Source rock and vitrinite studies in the Boorthanna Trough however indicate that the basal...-
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1982 seismic survey, Christmas Creek, final report.
AIM:The 1982 Christmas Creek Seismic Survey was designed to cover a wide area of the sparsely explored western farmout blocks of PELs 5 and 6, where Eromanga Basin sediments thin and overly sub-basins of variously aged prospective sediments. Primary...-
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Pedirka Sector: a reassessment of geology, porosity, maturity and maturity history.
A review of the Permo-Triassic and Mesozoic distribution of reservoir units. Data for some Birdsville Track Ridge wells are included as the development of the Pedirka Sector basins and the Birdsville Track Ridge are closely related.-
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Arckaringa Block. Farmout block progress reports from November 1982 to January 1989.
Exploration from 1982 includes: Christmas Creek - ARC Seismic Survey (see Envs 4808 and 5064),. Hogarth - ARC Seismic Survey, . Morphett - ARC Seismic Survey,. drilling of 2 wells (Birribiana 1 and Hans Knob 1), (see Envs 7034/6 and 7043/6)....-
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Published: 01 Jan 1989
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Organic petrology of samples from a selected group of wells in or near the Arckaringa Block.
Nineteen drill cuttings and 15 drill core samples of Permian, Cretaceous and Jurassic ages were assessed for organic maturation and source rock potential.-
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Organic petrology of samples from a selected group of wells in or near the Arckaringa Block.
34 selected drill core and cuttings samples from six wells were assessed by petrographic methods for their degree of organic maturation and petroleum source potential. The sampled sequence ranged in age from ?Devonian through to Permian, Jurassic and...-
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Bulgunnia. Progress reports and final report to licence full surrender, for the period 22/5/1978 to 10/8/1981.
The base metal and uranium potential of a concealed Proterozoic basement high near Bulgunnia Homestead was evaluated using geological and hydrogeochemical reconnaissance and regional geophysical interpretation approaches. Seismic, ground magnetic and...-
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ExpNotes CURDIMURKA: Explanatory Notes CURDIMURKA
There is no abstract created for this record-
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ExpNotes GILES: Explanatory Notes GILES
Concealed basement on GILES comprises ?Archaean to Palaeoproterozoic metamorphic rocks belonging to the Nawa Subdomain of the Gawler Craton. These are intruded by Mesoproterozoic Hiltaba Suite granitic bodies and Mesoproterozoic or Neoproterozoic...-
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ExpNotes WINTINNA: Explanatory Notes WINTINNA
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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The Lake Eyre Project. Joint first annual report plus final report to project licences' joint full surrender, for the period 3/5/2011 to 7/3/2013.
A large area surrounding the southern end of Lake Eyre, which is known to be underlain by a thinning succession of Cretaceous basinal sediments, was taken up to explore for possible economic secondary sandstone-hosted uranium mineralisation. No field...-
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Published: 27 Mar 1913
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RB 2006/00001 Guide to the sedimentary cover of the central Gawler Craton, South Australia
The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...-
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Published: 01 Jan 2006