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Uranium ore-forming systems of the - Geoscience Australia

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<strong>Uranium</strong> <strong>ore</strong>-<strong>forming</strong> <strong>systems</strong> <strong>of</strong> <strong>the</strong> Lake Frome regionLocality 3 (340434E ; 6647484N ) Mount Oliphant Plaque —Taking <strong>the</strong> track from Arkaroola Tourist Resort a few kilometers to <strong>the</strong> north <strong>the</strong>re is a plaquededicated to Sir Mark Oliphant.A walk 50m to <strong>the</strong> south from <strong>the</strong> plaque along <strong>the</strong> track a small cutting exposes a section <strong>of</strong> <strong>the</strong>Woodnamoka Phyllite showing retrogressed andalusite crystals, evident as quartz–muscoviteaggregates. This indicates amphibolite-facies metamorphism in contrast to little evidence <strong>of</strong>metamorphism at Arkaroola. The degree <strong>of</strong> metamorphism has <strong>the</strong>ref<strong>ore</strong> increased markedlyover <strong>the</strong> 3km northwards from Arkaroola, as <strong>the</strong> basement inlier is approached. Scapolite,tremolite and corderite isograds are essentially concordant with <strong>the</strong> unconformity.The increased strain can be seen in <strong>the</strong> Woodnamoka Phyllite compared to <strong>the</strong> earlier unitinvestigated.Page 127 <strong>of</strong> 151

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