Tectonic environment of shale-hosted massive sulphide Pb-Zn-Ag deposits of Proterozoic northeastern Australia
The large shale-hosted massive sulfide Pb-Zn-Ag deposits of the North Australian craton occur within basins that evolved in a continental setting in the overriding plate of a major subduction zone. The evolution of these basins is characterized by ∼ 140
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|Source:||Economic Geology; Bulletin of the Society of Economic Geologists|
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