Report Book 2010/5
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The Nullarbor Regional Reserve stretches from the western edge of the Gawler Craton at the boundary of the Yellabinna Regional reserve, south of the Trans Australian Railway and west to the WA border.
Prospectivity analysis is challenging due to limited basement outcrop and drilling, and low resolution geophysical data. The conclusions of this report and the degree of confidence in the evaluation are therefore very low in some areas resulting in an unknown mineral potential.
The Reserve is located in the Tertiary Eucla Basin which overlays the Officer Basin, the western margin of the Gawler Craton and the majority of the poorly known Coompana Block.
Four mineral systems are recognised as having the highest priority for mineral exploration. In the basement rocks these include orogenic gold and/or copper–gold, intrusive nickel–copper and iron ore. In the younger near surface environment within the Eucla Basin Tertiary landscape there is a high prospectivity for heavy mineral sand (HMS) deposits. A lower prospectivity zone is recognised in the central portion of the Nullabor Regional Reserve, in part due to lack of information, but also reflecting the higher prospectivity for intrusion-related mineral systems around geophysical basement targets, and HMS potential to the east.