Ongoing exploration for possible economic sandstone-type uranium deposits formed in Tertiary palaeochannels in the Yarramba area, 50 km north-west of Cockburn, has included further open hole rotary drilling and downhole geophysical logging (176...
Ongoing exploration for possible economic sandstone-type uranium deposits formed in Tertiary palaeochannels in the Yarramba area, 50 km north-west of Cockburn, has included further open hole rotary drilling and downhole geophysical logging (176 holes for a total penetration of 68, 232 feet, which included 145'6" of coring carried out in 3 holes that were re-drilled near the recent 580/1 uranium mineral discovery), plus the conduct of IP and ground magnetic surveys. During an initial phase of close-spaced drilling, extensions to the known mineralisation were found occupying a sinuous north-east trending zone along the target palaeochannel, including a high grade intercept made in hole 580/70 at the base of the Tertiary section, but although this mineralisation was found within channel bank sand over a reasonable (10' thick) depth interval, it was limited in width, and was not considered to be an economic proposition. However, during the final quarter of half-mile spaced exploratory drilling activity a more significant pod of uranium mineralisation was discovered in a probable tributary channel entering the main palaeochannel from the south-east. Here one 1' and two 2' thick bands of high grade (90,000 cpm) mineralisation occur over an area of at least 2 square miles, with two apparently differing phases of formation hosted by separate lithologies, both centred around the unconformity between the Tertiary sequence and the weathered Precambrian basement.
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