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RB 88/00019 Stratigraphic and tectonic overview of the Adelaide Geosyncline, South Australia.
The Adelaide Geosyncline contains an extremely thick folded Late Proterozoic to Middle Cambrian sequence deposited initially in rifted troughs and later in broad zones of regional subsidence. Age constraints on deposition are based on dating of rare...-
Document
Published: 01 Mar 1988
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AMIRA Project P544: Proterozoic sediment-hosted copper deposits. Quarterly progress reports and final report for the period July 2000 to October 2003.
The original objectives of this project were: 1) To understand the processes responsible for transporting, concentrating and fixing copper and other ore constituents during sedimentary basin evolution 2) To document the various stages and paragenesis...-
Document
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Bull 053 The Adelaide Geosyncline: Later Proterozoic Stratigraphy, Sedimentation, Pataeontology and Tectonics
The extremely thick succession provides one of the most complete sedimentary records for the Late Proterozoic. The term geosyncline is used in a non-genetic sense for the basin in which deposition occurred during the Adelaidean and Cambrian. Only the...-
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RB 2005/00008 Age, Origin and Emplacement of the Oodla Wirra Volcanics
A field mapping project was set up by PIRSA to investigate the age, origin and emplacement history of newly discovered [by Goldstream Mining NL on EL 2222] volcanic rocks within the Mount Grainger Anticline, close to the town of Oodla Wirra. Outcrop...-
Document
Published: 01 Jun 2005
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RB 2014/00006 Geology of the Cultana 1:100 000 map sheet (6432).
The revised digital geology map of the Cultana 1:100 000 map sheet and accompanying geological descriptions in this report are the first components of the 2nd edition PORT AUGUSTA 1:250 000 map sheet to be completed. The subject map sheet occupies the...-
Document
Published: 01 Jan 2014
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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...-
Document
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...-
Document
Published: 01 Oct 2009
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Interpreted basement geology to the Murray Basin and surrounds.
The purpose of this interpretation is to provide an initial framework for the basement to the Murray Basin upon which to plan the Geological Survey of South Australia’s MinEx CRC National Drilling Initiative drilling project targeting the Delamerian...-
Map
Published: 07 Jul 2020
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Cultana basement regional geology 3D Model.
The Cultana basement 3D Geological Model covers a region which includes the Roopena, and western half of the Cultana, 1:100,000 mapsheet areas. The subsurface geology that has been modelled comprises a succession of deformed Palaeoproterozoic...-
Model
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- ZIP
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ExpNotes MARREE: Explanatory Notes MARREE
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...-
Document
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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (3D pdf version 1)
Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...-
Model
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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (GOCAD version 1).
Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...-
Model
- ZIP,
