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The continuation during 2010 of exploration of the Palaeoproterozoic bedrock in a small area located 60 km west-northwest of Cowell has mainly consisted of the conduct of three shallow drilling campaigns and the examination and analysis of downhole...

A area centred ~ 25 km west of Cleve is being explored for possible buried economic sediment-hosted or basement unconformity - related uranium mineralisation. The tenement covers part of the Driver River and Driver River Pan which contains a...

A licence area originally comprising three separate sub-blocks located along the northern and southern sides of the Lake Gilles Conservation Park has been explored by grant licensee Lincoln Minerals Ltd (LML) and its joint venture partner IronClad...

Formal mining proposal documents submitted to PIRSA for approval as part of the process of re-opening the Uley graphite mine to sustain a planned 10 years duration open pit mining operation.

The subject very small licence area, located approximately 25 km north-west of Cleve, and which lies within the northern part of the NNE trending Kimban Campoona Syncline region located on central Eyre Peninsula, has been explored, in concert with...

An area of the southern Gawler Craton, which is located on Eyre Peninsula east of Elliston, is continuing to be explored for possible economic buried Archaean to Proterozoic bedrock-hosted primary base and precious metal deposits of inferred...

A licence composed of four separate small sub-blocks which generally lie ~90 to 120 km north-northeast of Port Lincoln is being explored primarily for extensions to known graphite-bearing horizons which may exist to the north and south of the...

A small area centred ~ 19 km west-northwest of Cleve was taken up primarily to explore for possible economic buried graphite mineralisation that might have formed within highly metamorphosed bedrock sediments located adjacent to large crustal...

An area centred ~30 km north-west of Cowell has been explored for possible buried graphite mineralisation that might have formed within highly metamorphosed Archaean to Proterozoic bedrock sediments located adjacent to large crustal penetrating...

An area in the Cowell Hills centred ~20 km north of Tumby Bay on eastern Eyre Peninsula was taken up primarily to explore and evaluate known talc and graphite occurrences, but the grant licensee's initial review of previous exploration data revealed...

A very small (35 square km) area located ~35 km west-northwest of Olary and covering part of the Weekeroo Inlier is being explored for possible buried epigenetic stratiform Broken Hill type Pb-Zn-Ag and VHMS (volcanic hosted massive sulphide) style...

An area located in the Lincoln Uplands of eastern Eyre Peninsula, immediately west of Port Neill, is being explored for possible economic shear-hosted polymetallic gold and base metal mineralisation that may be associated with the Kalinjala Mylonite...

The central portion of EL 5791 covering 77 square km or half of the originally granted licence area has been relinquished due to its now perceived diminished prospectivity for economic graphite, cobalt or zinc mineralisation. No field work was done on...

Exploration Licence 5870 ‘Carpie Puntha’, held by Archer Exploration Limited (Archer) is located on the eastern Eyre Peninsula within the Cleve Domain of the Gawler Craton. The presence of the Middleback Jaspilite provides for a small range of...

Two portions which constitute the majority of the two sub-blocks which form EL 5791, together covering 63 square km or ~82% of the formerly held area, have been relinquished due to their now perceived diminished prospectivity for economic graphite,...

Historically, exploration undertaken for finding Iron Oxide - associated Copper-Gold (IOCG) mineralisation on the eastern Gawler Craton, over the long period since the discovery of the Olympic Dam deposit in July 1975, has targeted positive gravity...

Most of a small licence area located ~19 km west-northwest of Cleve has been surrendered following the completion of a helicopter-borne EM survey over the entire tenement during July 2012, looking for signs of possible buried graphite mineralisation...

An area covering the northern end of the Campoona Syncline is being explored for possible economic buried graphite formed within Palaeoproterozic schistose rocks, which may exist as northern extensions to the Central Campoona graphite resource as well...