-
RB 75/00002 Notes on the TARCOOLA 1:250 000 preliminary geological map.
There is no abstract created for this record-
Document
Published: 09 Jan 1975
-
RB 74/00177 Progress report on the geology of the COOBER PEDY 1:250 000 sheet area (pre-Quaternary).
The Coober Pedy 1:250 000 sheet area (COOBER PEDY) is bounded by latitudes 29°S and 30°S and by longitudes 133°E and 135°E in the arid north of South Australia. The only town is the opal mining town of Coober Pedy on the northeastern margin of the...-
Document
Published: 01 Jan 1974
-
RB 75/00132 Tarcoola-Alice Springs railway. Engineering geology, Marla Bore to Baystone Bore section.
There is no abstract created for this record-
Document
Published: 01 Jan 1975
-
RB 2013/00011 Geology of the Tieyon 1:100 000 map sheet (5645).
The Tieyon 1:100 000 mapsheet area is located on the South Australia – Northern Territory border in the central Far North of South Australia. It covers rock units of the Mesoproterozoic Musgrave Province, the Mesozoic Eromanga Basin and the Neogene...-
Document
Published: 01 Apr 2013
-
Mount Treloar (NW of Oodnadatta). Progress and final reports for the period 30/6/80 to 29/12/80.
Follow-up investigations of possible buried channel redox front uranium mineralization on the edge of the Eromanga Basin, in the vicinity of the SA-NT border, included a geophysical and structural interpretation of available data, the drilling and...-
Document
Published: 23 Feb 1981
-
Mount Woods. Combined first progress/final report at licence full surrender, for the period 6/9/1979 to 5/12/1979.
Following an evaluation of existing subsurface data, 9 vertical percussion holes totalling 670 m were drilled to test discrete gravity anomalies in the Mount Woods area, in a search for Olympic Dam type mineralisation. The holes encountered...-
Document
-
Giddi Giddinna Creek. Progress and final reports for the period 3/3/1975 to 16/9/1975.
Fourteen rotary holes were drilled totalling 1362 metres. Coal was intersected as thin stringers in the Cretaceous Cadna-owie Formation in MU-3 and MU-13, and as a 1 metre thick seam in the Permian Mount Toondina Formation in MU-2, but is not...-
Document
Published: 01 Aug 1975
