Typization of ore-bearing carbonate-quartz veins and their connection with granitoids in the north of the Taimyr Peninsula
Abstract
In recent years, numerous quartz and carbonate-quartz veins with polymetallic mineralization have been identified in the north of the Taimyr-North-Earth folded region within the Mininsko-Bolshevist myogeosynclinal structural-formation zone.
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References
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