Geological structure of one of the polymetallic deposits of the Southern Altai
Authors:
Abstract
Southern Altai is a promising polymetallic region of Altai. Seven deposits and a large number (about 100) of points of lead-zinc and copper mineralization have been discovered within its limits. The polymetallic mineralization is spatially closely related to deposits of the Kultabar Formation of the Koblenzian‑Eifelian age. Younger and older sediments are generally of little interest with respect to polymetallic mineralization. Thus, the Kultabar Formation is the main ore-bearing sequence of polymetallic mineralization in the Southern Altai.
Область исследования:
Geology
Funding:
None
References
- Kazanin Yu. I. Polymetallic mineralization of the northeastern part of the Southern Altai. Izvestiya AN Kaz. SSR, seriya geologicheskaya, 1958, vol. 1. (in Russian)
- Khisamutdinov M. G. About influence of host rocks and temperature of solutions on composition and place of ore formation on the example of some Altai deposits. SSovetskaya geologiya, 1956, p. 50. (in Russian)