On the structures of the ore field of the cobalt-copper deposit
Authors:
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 ...
Область исследования:
(Archived) Without section
Funding:
None
References
- Velikiy A. S. Structures of ore fields. Izd-vo LGU, 1961.
- Knyazev I. I. Hydrothermally altered carbonate rocks. In the collection: Altered Near Ore Rocks and Their Prospecting Significance V sbornike Izmenennye okolorudnye porody i ikh poiskovoe znachenie. Gosgeoltekhizdat, 1954.
- Korolev A. V. , Shehtman P. A. Structural Conditions of Postmagmatic Ore Location. M., Nedra, 1965.
- Krivenko A. P., Pavlov A. N. Magmatic complexes of the Devonian trough of Tuva. Tr. IGiG SO AN SSSR, vol. 33, 1963.
- Krivenko A. P. Questions of Origin of the Torgalyk Intrusive Complex of Tuva. V sb. Magmaticheskie formatsii Altae-Sayanskoy skladchatoy oblasti. Moscow, Nauka, 1965.
- Pronin A. V. Statistical processing in stereographic projection of oriented values. Sov. geologiya, No. 37, 1949.
- Pek A. V. Fracture tectonics and structural analysis. Izd-vo AN SSSR, 1939.
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