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RB 90/00014 Explanatory Notes for the TALLARINGA 1:250 000 geological map.
There is no abstract created for this record-
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Published: 01 Mar 1991
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ExpNotes WINTINNA: Explanatory Notes WINTINNA
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
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RB 2019/00006 Sedimentology of the late Palaeozoic sedimentary rocks of the Arckaringa Basin, South Australia
Late Palaeozoic sedimentary rocks of the Arckaringa Basin in northern South Australia include diamictite and sandstone units of the Boorthanna Formation that were deposited as lodgement till under fluvioglacial conditions. The clast size and matrix...-
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Published: 01 Apr 2019
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RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
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Published: 01 Mar 2015
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Report of investigations for coal in the Arckaringa Basin, [conducted during the period] September to December 1974.
TARGET: Lower Permian coal of steaming or coking grade, suitable for open cut development. EXPLORATION: Rotary drilling of 42 open and partly cored holes totalling 5122 m, including 105 m of coring, with follow-up geophysical logging. RESULTS: 7...-
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ExpNotes COOBER PEDY: Explanatory Notes COOBER PEDY
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ExpNotes TALLARINGA: Explanatory Notes TALLARINGA
There is no abstract created for this record-
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ExpNotes WARRINA: Explanatory Notes WARRINA
The Peake and Denison Inliers (comprising the Davenport Range, Denison Range and small basement inliers to the east) form the dominant geological structure on WARRINA. The Inliers include outcrops of Palaeoproterozoic metamorphic basement which is...-
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