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Lake MacFarlane. Combined first annual / final report at licence expiry/full surrender, for the period 20/1/2016 to 19/1/2017.
Laboratory analysis of 18 samples of groundwater seepage brine collected from Lake MacFarlane during June-July 2016 indicated that the lake was unlikely to host an economically viable potash resource, and therefore the mineral exploration licence...-
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Published: 30 Nov 1916
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Bull 041 Geology and Mineral Resources of the Andamooka and Torrens Area
Regional geological mapping of the area was initiated in 1959 and was completed in 1964. All tracks in the area were traversed and detailed mapping confined to critical localities and to areas where this was considered desirable. Geological boundaries...-
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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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RB 61/00102 Geology and mineral resources of the Andamooka-Torrens area (19/10/1965).
The area embraced by the Andamooka and Torrens 4-mile geological sheets is defined by long 136° 30- long 138° 00 and lat 30° 00- lat 32° 00 and comprises an extensive partially dissected plateau west of Lake Torrens, the Lake Torrens sunkland and part...-
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Published: 19 Oct 1965
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Lake Torrens Areas 1 and 2, Lake Torrens South and Lake Torrens North (the Lake Torrens Brine Potash Project). First joint annual report plus final report to licences' joint full surrender, for the period 5/1/2015 to 16/6/2016.
Much of the eastern side of the very large, 5,745 square km saline playa Lake Torrens, which occupies one of the most arid parts of Australia, was taken under licence by a Northern Territory - based company with the intent of systematically sampling...-
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Published: 14 Jun 1916
