Drilling of fourteen exploration holes has been completed to date within the subject licence area, in a search for economic roll-front uranium occurrences within Tertiary sediments. Based on the current available data, the eastern portion of the...

As part of a wider search over SA for possible continental salt lake occurrences of NaCO3-rich brines and of fossil crystalline trona beds, presumed to be equivalent to the Lake Magadi (Kenya) / Green River Basin (Utah - Wyoming) style Tertiary...

As part of a regional search for possible economic sodium carbonate (trona) evaporite mineralisation formed within buried Miocene lacustrine sediments in an area located east of Lake Torrens, ground magnetic and gravity surveys were run along four...

Two small peripheral areas of the subject licence have been relinquished owing to their perceived poor potential for containing economic palaeochannel uranium mineralisation within Tertiary sediments. The western area is seen as being almost devoid...

Two peripheral areas of the subject licence have been relinquished owing to their perceived poor potential for containing economic palaeochannel uranium mineralisation within Tertiary sediments. Two rotary mud drillholes were drilled in the western...

Diamond drillhole WC1 was drilled by Marathon to a total depth of 173.5 m over the Woolatchi Creek aeromagnetic anomaly, as part of an ongoing search for uranium and base metals in the north-eastern Flinders Ranges and Lake Frome Plains region....

Approved PACE project DPY2-11 was an attempt to find calcrete or roll-front type sedimentary uranium mineralisation in Quaternary fluvial channels that drain the northern and eastern margins of the uranium-enriched Mount Painter and Mount Babbage...

41 open-hole rotary drillholes (total 5999 metres) were drilled and geophysically logged to search for possible sedimentary uranium occurrences in the Early Cretaceous Parabarana Formation and in overlying altered Miocene sands, over an area of the...

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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...