Lime magnesite rough. LMR 102 purple chalcedony The quartz epidote axinite mineralisation
Description
The quartz epidote axinite mineralisation was evidently caused by hydrothermal activity related to the doleritic sills which are in close proximity to the occurrence
8 billion years
From an unassigned unit of the Wyloo Group
GRN86 Green Opal & Magnesite slab
Dimensions at widest points approximately 140 mm x 90 mm x 8 mm thick
Lime magnesite rough. LMR 102 purple chalcedony The quartz epidote axinite mineralisationLMR102 Rough Lime Magnesite suitable for cabbing, tumbling or specimens. Dimensions at widest points approx. 110 mm x 80 mm x 30 mm Weighs 522 grams From north of Kalgoorlie , Western Australia.
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