The true width of the intervals is unknown. The elevated PGEs are associated with disseminated sulphides in predominantly serpentinised ultramafic intrusive rock-types. Base metal assays for the hole are pending. No conductive zone was intersected in JRC004 to explain the presence of Conductor ‘C’. However, asubsequent DHEM survey has identified a strong off-hole conductor (‘C1’), consistent with a massive sulphide source, modelled to be about 30m below JRC004.
Reuters article on re palladium, page-14
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