Mineralisation at Aurora is different to established Platreef-type mineralisation.
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Base metal sulphides are hosted by leucocratic not melanocratic rocks.
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Pigeonite and orthopyroxene co-exist in the mineralised zone.
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Mineralogy and geochemistry are consistent with the Upper Main Zone.
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Aurora-type mineralization may be traced along strike for > 20 km to north and south.
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