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RB 50/00014 Report on quartzite deposit, secn 128 Hd Dalkey - Highways and Local Government Department.
A ridge composed of massive grey-blue to pink quartzite occurs 3½ miles north-north-west of Owen Railway Station. The deposit is regarded as belonging to the River Wakefield sandstones and shales of the Wlllouran series. The beds dip 25 to 30 to the...-
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Published: 01 Jan 1960
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RB 50/00181 Quartzite deposit, secn 128 Hd Dalkey. Report on diamond drilling.
Owen Township has been tested by diamond drilling to prove its suitability for road building. Reserves in excess of 50 000 cubic yards of good quality quartzite suitable for use as crushed aggregate have been indicated.-
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Published: 18 May 1960
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RB 81/00089 Copper mineralization in the Eurelia Carrieton area.
Uneconomic stratiform copper mineralization over area of 2.5 by 1 km was discovered by Utah west of Eurelia in 1969 - 1977. It occurs near core of SW plunging anticline in the Burra Group. Host rocks are carbonaceous and pyritic siltstone, dolomite,...-
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Published: 01 Jan 1981
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RB 76/00134 Geochemical exploration of the Riverton and Eudunda 1:63 360 sheets. Completion report.
About 1,500 samples were collected during a stream sediment sampling survey on the Riverton and Eudunda 1:63 360 geological sheets and analysed for Cu, Pb, Zn, Au, W, Mo, Nb, Co and Mn. Rolling means, residual values, correlation coefficients and mean...-
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Published: 01 Jan 1976
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RB 76/00156 Bungaree Quartzite (new name). Lower Adelaidean, southwest of Spalding, South Australia.
Mapping near the Spalding Inlier and to the south indicates that a quartzitic sequence between the River Wakefield Group (now termed Subgroup) and Skillogalee Dolomite was wrongly identified as Rhynie Sandstone and should now be re-named. The term...-
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Published: 15 Dec 1976
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RB 93/00042 Orroroo bedrock drilling 1993.
Eighty three reverse circulation drill holes totalling 2615.5 metres were drilled on Quorn, Orroroo, Paratoo and Carrieton 1:100 000 sheets to determine bedrock geology and geochemistry below sedimentary cover. The program is a part of the South...-
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Published: 01 Oct 1993
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RI 036 The Geology of the 0rroroo 1:250,000 Map Area
There is no abstract created for this record-
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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 68/00020 Precambrian stratigraphic sections near Spalding, Yatina, Carrieton and Manna Hill, South Australia.
Eight stratigraphic sections were measured on enlargements of air photos between Spalding and Cradock, up to 200 miles north or northeast of Adelaide. The rocks are mainly from the Umberatana, Burra and River Wakefield Groups of the Adelaide System....-
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Published: 20 Feb 1969
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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 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 62/00034 Geology of the Spalding Willouran Inlier.
The Spalding inlier is a lens-shaped area of tightly-folded Willouran rocks of the Adelaide System (Upper Precambrian), extending north-south for about 10 miles; it is about 100 miles north of Adelaide. The rim of the inlier is marked in most places...-
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Published: 09 Feb 1966
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RB 73/00311 River Broughton Beds - A Willouran sequence in the Spalding Inlier.
The Spalding Inlier, about 150 km north of Adelaide, is the core of a faulted anticlinorium providing a unique exposure of some of the oldest sediments in the southern half of the Adelaide Geosyncline. The discovery of stromatolites within the inlier...-
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Published: 24 Dec 1973
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RB 2007/00006 The geology and mineral potential of the PORT AUGUSTA [mapsheet] area, eastern Gawler Craton.
The PORT AUGUSTA 1:250,000 mapsheet area covers the north-eastern part of the Eyre Peninsula, the northern Spencer Gulf and the south-western Flinders Ranges, and extends from latitude 32°00'S to 33°00'S and longitude 136°30'S to 138°00'S. The main...-
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Published: 01 Apr 2007
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RB 2016/00013 Geological field excursion guide — Rifts, reverse faults and regolith: Neoproterozoic to Cenozoic geology in the Mid-North of South Australia.
The rolling hills, wheat paddocks and vineyards of the Mid-North region of South Australia conceal a geological transition between the Adelaide Hills and the Flinders Ranges. Here the landscape is subtly controlled by the Neoproterozoic bedrock...-
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Published: 01 Jul 2016
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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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