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Regional Geology
▪ Hemi in the Archaean Pilbara Craton
▪ Broad ENE trending greenstone and meta-sedimentary sequence
▪ Complex folding and deformation
▪ Mallina Formation sediments
▪ Intruded by Langenbeck mafic-ultramafic sills and felsic to intermediate granitoids (Mt Dove Granite)
▪ Major structural corridors – Tabba Tabba shear zone and Mallina shear zone
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