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RI 035 Geology of The Beltana 1:63,360 Map Area
Includes Palaeontological report on Nilpena limestone. Appendix 3 in: Leeson, B.-
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RI 028 The Geology of the Marree 1:250,000 Map Area
There is no abstract created for this record-
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ExpNotes CURDIMURKA: Explanatory Notes CURDIMURKA
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ExpNotes COPLEY: Explanatory Notes COPLEY
There is no abstract created for this record-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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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 66/00162 Progress report on the geology of the Winnininnie 1:63 360 map area.
Mapping of the Winnininnie 1:63,360 mapsheet has been undertaken as part of a programme to complete mapping of the Olary 1:250,000 Sheet. The area lies about 200 miles from Adelaide on the road and railway line to Broken Hill, and includes the...-
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Published: 01 Jan 1968
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RB 63/00133 Subdivision of the Adelaide System (submitted to 39th ANZAAS Congress Precambrian Symposium, secn C).
There is no abstract created for this record-
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Published: 01 Jan 1966
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RB 65/00047 Stratigraphic section measurement and sections near Spalding and Port Augusta.
A programme of stratigraphic section measurement is envisaged in order to facilitate rock correlation and help outline the pattern of sedimentation in the Adelaide Geosyncline. In many areas measurement may be made on air photo enlargement, as has...-
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Published: 01 Jan 1967
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RB 66/00074 Geology of the ORROROO 1:250 000 map area.
An essentially unmetamorphosed sequence of Upper Proterozoic Adelaide System rocks has been folded into a parallel series of north and north-east trending folds on the ORROROO mapsheet area. Rocks of the Adelaide System are up to 50,000 ft thick, and...-
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Published: 01 Jan 1971
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RB 71/00178 Explanatory Notes for the COPLEY 1:250 000 geological map.
The COPLEY 1:250 000 map area includes the northern Flinders Ranges and the southern part of the Willouran Ranges. It is bounded to the west by the Lake Torrens Sunkland and, to the east, by the Lake Frome Plains. A thick sequence of older Precambrian...-
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Published: 08 Nov 1971
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RB 71/00203 Geochemical survey of the Mount John-Paralana Fault Zone. Third report.
Seven holes drilled to a maximum depth of 195 ft. (59 m) tested part of the Mt. John Paralana Fault zone for mercury. No anomalous concentrations of mercury were detected. Three holes tested the Parachilna Formation west of the Moro Mine. Anomalous...-
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Published: 01 Jan 1973
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RB 73/00126 International Union of Geological Sciences, Subcommission on Precambrian Stratigraphy. Notes for excursions in South Australia 1973.
Brief geological information is given for points to be visited over eight days as illustration of the Adelaide System in South Australia, with an emphasis on Adelaidean glacigene rocks. The Callanna Beds are seen in the Arkaroola region, the Aldgate...-
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Published: 01 Jan 1973
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RB 72/00161 Explanatory Notes for the LINDSAY 1:250 000 geological map.
The LINDSAY 1 :250 000 sheet area occupies parts of the southern Musgrave Block and the northern Officer Basin, in the North West Province of South Australia. It is entirely contained by the Great Victoria Desert. The oldest rocks are gneisses of...-
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Published: 21 Aug 1972
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RB 70/00037 Progress of mapping in the Olary region.
Adelaidean and younger rocks of the Yunta, Winnininnie, Oakvale, Mutooroo, Ballara, Wadnaminga, Olary and Manunda one mile areas are summarised.-
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Published: 25 Feb 1970
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RB 61/00130 Preliminary report on the Precambrian stratigraphy of the Carrieton 1-mile sheet.
The Carrieton 1:63, 360 map area lies about 200 miles north of Adelaide, South Australia. It contains folded rocks of the Burra, Umberatana and Wilpena Groups of the Adelaide System, of Upper Precambrian age; total thickness of these rocks exceeds...-
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Published: 01 Jan 1965
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RB 63/00058 Geology of the Beltana 1:63 360 map area.
Rocks belonging to the upper part of the Adelaide System and the overlying Cambrian, outcrop in the eastern part of the Beltana area in the Nuccaleena Dome, and form the basement underlying the more recent sediments to the west. In the central and...-
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Published: 01 Jan 1970
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RB 75/00013 Stratigraphic sections through the uppermost Umberatana Group near Yunta and Manna Hill, South Australia.
There is no abstract created for this record-
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Published: 01 Jan 1975
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RB 76/00029 Stratigraphic section across the Umberatana Group-Wilpena Group boundary, near Horrocks Pass in the Wilmington area.
A section was measured across the Umberatana Group - Wilpena Group boundary near Wilmington in the Southern Flinders Ranges, on the western margin of the Adelaide Geosyncline. Grey red massive siltstones are correlated with the Reynella Siltstone...-
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Published: 04 Mar 1976
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Merna Mora. Annual reports to licence expiry/full surrender, for the period 9/10/2006 to 8/10/2013.
A small licence area located on the Flinders Ranges piedmont plain south-east of Lake Torrens was taken up by Jim Allender to investigate the IOCG potential of a discrete regional gravity anomaly which he had identified from data in the public domain,...-
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Published: 20 Nov 1913