On the structures of the ore field of the cobalt-copper deposit
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Abstract
The ore field of the cobalt-copper deposit is confined to the zone of juxtaposition of large tectonic structures: the East-Tannuol anticlinorium and the West-Tannuol synclinorium. They intersect along the Ubsunur-Bayapkol deep fault, which can be traced from southwest to northeast for more than 100 km. The Ubsunur-Bayankol deep fault is adjoined to the east by the 80 km long-lived Ungesh fault zone. The intersection of these regional faults controls cobalt-nickel arsenide and cobalt-copper sulphoarsenide mineralization of the ore field under consideration ...
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References
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