Olary Creek
(U3O8 Limited 100%)
- Major palaeochannel defined by gravity survey
The Olary Creek project is located some 250 kilometres north east of Adelaide and covers an area where younger Tertiary sediments on-lap Proterozoic basement along the northern margin of the Tertiary sequences on the edge of the Murray Basin are prospective for palaeochannel style uranium mineralisation (Beverley, Honeymoon) in drainages shedding from the nearby hardrock Radium Hill deposit which was the site of Australia's first uranium mine. Previous drilling located uranium mineralisation in the basal part of the Miocene sand sequence along the north-east trending Anabama-Redan fault zone and in a major tributary further north, close to the current course of Olary Creek. Most previous drilling focused on the Anabama Fault zone to the south of U3O8's tenement while the tributaries from the likely source region around Radium Hill which pass through EL3454 are lightly explored.
In an effort to clearly define the extent of the buried palaeochannel, U3O8 Limited completed a detailed gravity survey over part of the exploration licence. The gravity survey covered 80km2 for a total of 485 stations, 200 metres apart and along one kilometre east-west traverses.

The survey clearly defined a significant buried channel system with tributaries running into it. A drilling programme is planned to test the geological characteristics of the palaeochannel and the presence of uranium mineralisation. The programme will be completed in the December 2007 Quarter.
Processed Gravity Image highlighting probably palaeochannel
