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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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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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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
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Ediacara Range. Partial surrender report for the period ending January 1998.
Relinquished portions of the EL were considered to have low potential for economically viable Mississippi Valley-type lead mineralisation similar to that occurring at the Ediacara Mineral Field, a conclusion based on the outcome of literature...-
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Mount Michael. Annual report and final report to licence expiry/full surrender, for the period 7/9/1997 to 6/9/1999.
Interpretation of magnetic and gravity data, together with calcrete and MMI sampling, were carried out adjacent to a southerly extension of the Ediacara Fault, 25 km north-west of Parachilna. Low order Pb-Zn-Ag anomalism was located, coincident with...-
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Published: 10 Nov 1999
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Woolly Dam. Progress reports and final report to licence expiry/full surrender, for the period 9/1/1978 to 8/1/1980.
Exploration undertaken in an area of practically no outcrop that is situated north and north-west of the Ediacara Range, on the eastern side of Lake Torrens, has aimed primarily at investigating the mineral potential of a large, low amplitude...-
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Published: 05 Jun 1980
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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
- ZIP,
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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,
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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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