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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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Burial history analysis of the east Officer Basin, South Australia. A preliminary study.
In South Australia, the intracratonic eastern Officer Basin, which may contain up to 10 km of Neoproterozoic to Paleozoic sediments, is bounded by the Precambrian Gawler Craton to the southeast, the Musgrave Block to the north, and passes into...-
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Interpretation of apatite fission track data from the Officer Basin.
13 sedimentary rock samples from Proterozoic through to Mesozoic formations intersected in 5 Officer Basin wells yielded apatite fission track analysis data (track length and density) used to interpret, via statistical modelling, the broad geothermal...-
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Published: 21 Dec 1994
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Burial history of the eastern Officer Basin, South Australia.
Burial history analysis of the structurally complex eastern Officer Basin region was performed using data from petroleum, trona exploration and stratigraphic wells, seismic upholes, coal drillholes and selected seismic sections, to construct isopachs...-
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RB 2019/00006 Sedimentology of the late Palaeozoic sedimentary rocks of the Arckaringa Basin, South Australia
Late Palaeozoic sedimentary rocks of the Arckaringa Basin in northern South Australia include diamictite and sandstone units of the Boorthanna Formation that were deposited as lodgement till under fluvioglacial conditions. The clast size and matrix...-
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Published: 01 Apr 2019
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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
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
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Published: 01 Mar 2015
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Reedy Lagoon. Progress and final reports to licence surrender for the period 20/7/81 to 4/8/86.
Exploration as part of a continuing regional search for possible diamondiferous kimberlites was undertaken 70 km west-northwest of Roxby Downs. Extensive sampling of current drainage lines in interdune swales, plus loam sampling in other...-
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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 2013
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ExpNotes BARTON: Explanatory Notes BARTON, SH 53-09.
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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ExpNotes COOBER PEDY: Explanatory Notes COOBER PEDY, SH 53-06.
There is no abstract created for this record.-
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ExpNotes GILES: Explanatory Notes GILES, SH 53-01.
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, SG 53-14.
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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