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RB 2007/00011 Original full content version of] OOLDEA, South Australia, [geological map] sheet SH52-12. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The OOLDEA 1:250 000 map area, in the far west of SA, includes portions of the Maralinga Tjarutja Aboriginal Lands, Maralinga Prohibited Area, and Nullarbor Regional Reserve. It is traversed by the Trans-Australian Railway. There is no significant...-
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Published: 01 Jun 2007
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RB 2001/00021 Development of geoscientific models for exploration in Tertiary palaeochannels draining the north-western Gawler Craton, SA.
The precise geometric definition of palaeochannels on the north-western Gawler Craton, South Australia, is important in the exploration for placers (e.g. gold and heavy minerals), secondary geochemical deposits (e.g. uranium) and even for lignite and...-
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Published: 01 Dec 2001
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RB 2016/00025 Geology of the Peltabinna 1:75 000 Special Edition Map Sheet.
The Peltabinna 1:75 000 Map Sheet was produced as part of a mapping program integrated into the Mineral Systems Drilling Program (MSDP) along the southern margin of the Gawler Ranges. The objective of the mapping program was to provide a regional...-
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Published: 01 Sep 2017
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Geoscientific signatures of Tertiary palaeochannels and their significance for mineral exploration in the Gawler Craton region.
Tertiary palaeochannels of the northwestern Gawler Craton have become the focus of recent exploration due to the probable association between placer gold, heavy minerals, coal, uranium and groundwater resources, and channel sediments. The...-
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Regolith map of the southern Gawler Ranges margin (300 dpi & 600 dpi pdf formats).
This inaugural regolith map of the southern Gawler Ranges margin provides a valuable regional overview of the main regolith types and their associated landforms, plus a general outline of the major areas of bedrock or regolith-dominated terrain, as...-
Map
Published: 14 Jul 2016
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ExpNotes BARTON: Explanatory Notes BARTON
Shallow Precambrian crystalline basement underlies the greater part of the BARTON 1:250 000 map area. Thicker Neoproterozoic, Cambrian and Carboniferous Permian sediments occur in the northwest, with the southern margin bounded by the Karari Fault...-
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ExpNotes OOLDEA: Explanatory Notes OOLDEA
There is no abstract created for this record-
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