A licence area covering the piedmont plain formed adjacent to a large salt lake (Lake Blanche) of the Cenozoic Lake Eyre Basin, and the underlying Mesozoic Eromanga Basin sediments situated to the north of the uranium-rich Mount Babbage Inlier, ~100 km east of Marree, has been explored for possible economic lithium evaporite mineralisation that might exist in as shallow brine lenses within surficial sediments, as well as for possible buried Cenozoic roll front style sedimentary uranium mineralisation which could be associated with the northern reaches of the buried Blanchewater Palaeovalley that was mapped by Geoscience Australia using the data from its 2010 Frome Airborne Electromagnetic Survey. The only work performed by GBE consisted of a desktop review of the available open file geological and geophysical data for the area, plus the assessment of recent exploration results (including from drilling) obtained by explorers Red Metal and Cauldron Energy in neighbouring tenements. It was stated that there has been no known previous drilling done on the subject licence area. The licensee's interpretation of the Frome AEM survey data and the results from nearby drilling have served to indicate that the Eyre Formation sediments deposited in a number of local paleochannels probably have the following attributes: • they were hydrogeologically connected to felsic rocks enriched in leachable uranium (Yerila Granite in the Mount Babbage Inlier, and possibly Mount Neill Granite in the Mount Painter Inlier); • within them, the palaeo-groundwater flow direction away from the source area was broadly towards the north and north-east; and • because reduced Eyre Formation sediments were located in nearby drilling to the south, it is reasonable to assume that the locus of the potential redox front should lie towards the north, possibly on EL 5391.