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Assay results have demonstrated that the pegmatite dykes are fertile and mineralised with lithium and tantalum everwhere that they were intersected in drilling (see Table 1). Significant intersections of lithium mineralisation (see Table 2) typically occurred in continuous zones within the pegmatite dykes, which were up to 15 m true thickness. Continuity of the dykes was established over strike lengths of up to 200 m
I like this part. Assay results have demonstrated that the...
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