Definitely some anomalous base metal and PGE results at Hartog within the laterite horizon (which incidentally forms part of Alcoa's bauxite resources within the Julimar State Forest) BUT low-grade anomalism more likely indicates the upper levels of a primary igneous body AFTER the goodies have settled out towards the base of the chamber at Julimar (assuming my interpretation of lode geometry is ultimately upheld by detailed geo-metallurgical analysis of drilling).
Difficult to compare geochemistry at Julimar to Hartog as the profile at Julimar is stripped of laterite and terrane is excised by erosion. The high-grade PGE results in the oxide over Julimar exist within the lower saprolite horizon NOT the laterite. Different ranges need to be applied when referencing anomalism at different levels of the weathering profile!!
P
Definitely some anomalous base metal and PGE results at Hartog...
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