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1981 and 1982 seismic surveys, Wertaloona and Christmas Creek-ARR, final report.
Wertaloona Seismic Survey - AIM:The 1981 Wertaloona Seismic Survey programme was designed by the PELs 5 and 6 Arrowie Block partners to provide the first high quality, multifold seismic reflection data in the area of likely preserved thick Cambrian...-
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Arrowie Block acreage assessment.
During the period January 1946-December 1985 under review, the following petroleum exploration work was carried out over the Arrowie Block: 6 gravity, 2 aeromagnetic and 10 seismic surveys (total seismic coverage 2781 line km), plus 4 wells, all dry....-
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RB 63/00026 Determination of refraction seismic velocities in Proterozoic and Palaeozoic outcropping sections in Blinman-Wirrealpa area, Flinders Ranges.
To aid in the correlation of deep refractors in the Frome Embayment, a series of eight seismic refraction velocities were determined on the Proterozoic and Palaeozoic outcropping sections in the Blinman-Wirrealpa area of the Flinders Ranges. The...-
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Published: 01 Jan 1966
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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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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...-
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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
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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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