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Benagerie Ridge Areas A to E (initially the Curnamona IOCG Project, and later becoming part of the Curnamona South Uranium Project). Joint annual reports to licences' respective or joint (final) surrender, for the period 25/5/2005 to 9/6/2015.
Five conjoined exploration licences covering the buried central and northern Benagerie Ridge basement province that is comprised predominantly of Mesoproterozoic volcanic and intrusive rocks, have been explored for possible economic iron oxide -...-
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Published: 14 May 1915
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Data release [made at SA Director of Mines' discretion] : Hedley Hill. Annual reports submitted until the commencement of joint reporting for the six Lake Torrens Project licences, for the period 26/5/1997 to 25/5/2000.
Exploration Licence 2340 “Hedley Hill” is located adjacent to the northeast extremity of Lake Torrens. During the 80’s and 90’s exploration of the Lake Torrens district has had the prime objective of the discovery of an "Olympic Dam" style deposit...-
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Published: 20 Jul 1900
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Welbourn Hill. Second partial surrender report, for the period 15/1/2008 to 14/1/2016.
Approximately 66% of the former area of the subject licence has been surrendered in two separate portions together totalling 104 square km, due to perceived diminished prospectivity for possible buried Proterozoic IOCG-U deposits. During March 2015,...-
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RB 2004/00001 Palaeochannel studies related to the Harris Greenstone Belt, Gawler Craton, South Australia. Architecture and evolution of the Kingoonya Palaeochannel system.
Exploring the earth resources in the Harris Greenstone Belt (HGB) region is complicated by a regolith cover produced by a long and complex history of landscape evolution. The present surface of the HGB indicates little of the complex palaeochannel...-
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Published: 01 Jun 2004
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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 2001/00009 Downhole environmental risks associated with drilling and well completion practices in the Cooper/Eromanga Basins.
This project reviewed literature in order to: - evaluate any downhole environmental risks associated with drilling fluids and completion practices in the Cooper and Eromanga Basins; and - assess the effectiveness of cementing practices in achieving...-
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Published: 01 Mar 2001
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RB 2008/00012 Coober Pedy Opal Exploration Drilling Program 2005.
Two South Australian Government grants totalling $100 000 have been used by the Coober Pedy Miners Association Inc. to fund the use of an auger drilling rig on a drilling programme designed to explore for opal at selected locations away from the known...-
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Published: 01 Oct 2008
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RB 2008/00013 High Resolution Resistivity Test Survey: Coober Pedy.
A new high-resolution resistivity measurement instrument, developed by ZZ Resistivity Imaging Pty Ltd, was tested within the Coober Pedy Precious Stones Field, located 900 km north-west of Adelaide, to determine its suitability for assisting in opal...-
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Published: 01 Oct 2008
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RB 2015/00005 Opal Exploration Program — Andamooka Opal Fields.
Opal at Andamooka is found in the Bulldog Shale, a stratigraphic unit comprising shallow marine-deposited sediments of Cretaceous age. The opal mostly has formed within a bleached sediment weathering profile developed at the contact of a sandy...-
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Published: 01 Apr 2015
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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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Tieyon, South Australia. Sheet 5645, International Index. 1:100 000 Geological Series digital map.
Tieyon is located on the eastern margin of the Proterozoic Musgrave Province. The region includes rocks from two distinct geological provinces, the eastern limit of exposure of the Musgrave Province, and the north-western margin of the Mesozoic...-
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Published: 17 Sep 2013
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Ruby Hill. Progress and final reports to licence surrender for the period 1/12/1980 to 31/5/1982.
During a search for possible diamondiferous rocks within an area lying to the north of William Creek and abutting the south-eastern side of the Peake and Denison Ranges, stream sediment sampling and a low level, 5300 line km aeromagnetic / radiometric...-
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Published: 02 Jun 1982
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RB 2015/00007 Coober Pedy Precious Stones Field 40Ar/39Ar geochronology of alunite and opal formation.
Precious opal in South Australia occurs near the base of the weathered profile developed in Early Cretaceous host marine clastic sediments. It is associated with the supergene minerals alunite, kaolinite, gypsum and iron oxides, that are variously...-
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Published: 01 Apr 2015
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RB 2013/00011 Geology of the Tieyon 1:100 000 map sheet (5645).
The Tieyon 1:100 000 mapsheet area is located on the South Australia – Northern Territory border in the central Far North of South Australia. It covers rock units of the Mesoproterozoic Musgrave Province, the Mesozoic Eromanga Basin and the Neogene...-
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Published: 01 Apr 2013
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RB 2008/00008 Northern Curnamona Province, Regolith Exposures, Tour Guide.
The northern Curnamona Province includes the northern Flinders Ranges, comprising the Mounts Babbage and Painter Inliers (Palaeoproterozoic to Neoproterozoic crystalline basement) and overlying metasediments of the Adelaide Geosyncline...-
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Published: 01 Sep 2008
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
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Published: 01 Apr 2012
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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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RB 2010/00003 High Resolution Resistivity Test Survey: Andamooka.
A new high-resolution resistivity measurement instrument, developed by ZZ Resistivity Imaging Pty Ltd, was tested within the Andamooka Precious Stones Field, located 640 km by road north of Adelaide, to determine its suitability for assisting in opal...-
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Published: 01 Feb 2010
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Agnes Creek, South Australia. Sheet 5544, International Index. 1:100 000 [scale] Geological Map Series digital map.
Agnes Creek is located near the eastern outcrop margin of the Proterozoic Musgrave Province, which is composed predominantly of amphibolite to granulite facies meta-igneous and metasedimentary gneisses of the Birksgate Complex. Geochronological...-
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Published: 02 Jul 2018
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......[Key SAMREF record for accessing referenced reports and data via DEM Content Manager - SPOT]...... Mount Toondina. Annual reports and final report to licence surrender, for the period 13/2/1995 to 15/8/1998.
The Mount Toondina structure, a small but pronounced vertically fault-bounded inlier of Permian sediments within a flat-lying Mesozoic sequence, is represented by an annular magnetic feature located 45 km south of Oodnadatta. A single gravity profile...-
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