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RI 044 The Geology and Hydrocarbon Potential of the Pedirka Basin
Includes Permian palynology of Purni 1, Witcherrie and Mokari 1, Pedirka Basin.-
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Data release - as updated : Phar Lap Outstation. Annual reports plus final report to licence expiry/full surrender, for the period 27/8/2007 to 26/8/2017.
An area centred ~85 km south-southeast of Coober Pedy, at the southern margin of the Lake Phillipson Trough, a long active tectonic feature now occupied by deep sedimentary fill, was taken up by a wholly-owned subsidiary to Monax Mining Ltd primarily...-
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Published: 24 May 2017
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Peake Hill. Annual and final reports to licence expiry/full surrender, for the period 16/7/2007 to 15/7/2012.
An area located on and closely marginal to the Denison Inlier of the Proterozoic Peake and Denison Ranges, approximately 80 km south-east of Oodnadatta, was explored for possible roll-front style sedimentary uranium deposits that may have formed...-
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Published: 03 Aug 2012
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Boundary Dam. First partial surrender report, for the period 20/7/2007 to 19/7/2010.
A small licence area taken up approximately 130 km north of Marla, near the SA/NT state border, is being explored for possible economic secondary uranium mineralisation formed in sandstone or calcrete. Prior to Tianda Resources deciding to apply for...-
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Published: 27 Sep 2010
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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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ExpNotes ABMINGA: Explanatory Notes ABMINGA, SG 53-10.
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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ExpNotes TALLARINGA: Explanatory Notes TALLARINGA, SH 53-05.
There is no abstract created for this record.-
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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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ExpNotes PANDIE PANDIE: Explanatory Notes PANDIE PANDIE, SG 54-09.
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 CALLABONNA: Explanatory Notes CALLABONNA, SH 54-06.
There is no abstract created for this record.-
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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 CURDIMURKA: Explanatory Notes CURDIMURKA, SH 53-08.
There is no abstract created for this record.-
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ExpNotes MARREE: Explanatory Notes MARREE, SH 54-05.
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
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ExpNotes WARRINA: Explanatory Notes WARRINA, SH 53-03.
The Peake and Denison Inliers (comprising the Davenport Range, Denison Range and small basement inliers to the east) form the dominant geological structure on WARRINA. The Inliers include outcrops of Palaeoproterozoic metamorphic basement which is...-
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ExpNotes OOLDEA: Explanatory Notes OOLDEA, SH 52-12.
There is no abstract created for this record.-
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ExpNotes KINGOONYA: Explanatory Notes KINGOONYA, SH 53-11.
There is no abstract created for this record.-
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ExpNotes POOLOWANNA: Explanatory Notes POOLOWANNA, SG 53-12.
There is no abstract created for this record.-
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