-
Pinding. Annual reports and final report to licence expiry/full surrender, for the period 10/5/2004 to 24/8/2012.
An area centred approximately 30 km south-west of Tarcoola has been explored primarily for possible economic shear-hosted or epithermal/hydrothermal IOCG style Proterozoic gold, and for inferred Archaean magmatic nickel deposits associated with...-
Document
Published: 14 Sep 1912
-
RB 2004/00001 Palaeochannel studies related to the Harris Greenstone Belt, Gawler Craton, South Australia. Architecture and evolution of the Kingoonya Palaeochannel system.
Exploring the earth resources in the Harris Greenstone Belt (HGB) region is complicated by a regolith cover produced by a long and complex history of landscape evolution. The present surface of the HGB indicates little of the complex palaeochannel...-
Document
Published: 01 Jun 2004
-
RB 2006/00001 Guide to the sedimentary cover of the central Gawler Craton, South Australia
The central Gawler Craton is blanketed by thin sedimentary cover that ranges in age from Neoproterozoic to Quaternary. Locally, though, such cover can reach a maximum of ~500 m thickness in Permian glacial valleys or rift structures. This guide...-
Document
Published: 01 Jan 2006
-
RB 2007/00008 CHILDARA, South Australia, [geological map] sheet SH53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The CHILDARA 1:250 000 map area is located on the western Gawler Craton, an ancient crystalline shield comprising Archaean, Palaeoproterozoic and Mesoproterozoic metasediments, volcanics and granites that has been tectonically stable since 1450 Ma...-
Document
Published: 01 May 2007
