GOLD IN NEWFOUNDLAND
quartz-sulphide veins and quartz-carbonate shear zones in a variety of deformed metamorphic terranes. Orogenic gold systems occur in mid-Paleozoic slate belts developed in Ordovician and Silurian sediments. Cambro-Ordovician gold-bearing hydrothermal systems are typically associated with the formation of volcanogenic massive sulphide deposits.
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