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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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Yarley. Annual reports to licence expiry/full surrender, for the period 19/8/2009 to 18/8/2012.
A small area located on the southern Lake Torrens Plains immediately west of the ABC Range was taken up to allow evaluation of its potential for having buried economic sedimentary coal and/or uranium mineralisation occurrences. There are no...-
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Published: 02 Sep 1912
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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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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), SH 54-13.
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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