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Металлогения Камчатского срединного массива
Author(s) -
V. A. Stepanov,
V. Ye. Kungurova,
I. A. Koidan
Publication year - 2020
Publication title -
vestnik severo-vostočnogo naučnogo centra dalʹnevostočnogo otdeleniâ ran
Language(s) - English
Resource type - Journals
ISSN - 1814-0998
DOI - 10.34078/1814-0998-2020-4-39-54
Subject(s) - copper , mineralization (soil science) , massif , geology , geochemistry , molybdenum , nickel , sulfide , quartz , igneous rock , sulfur , metallurgy , materials science , paleontology , soil science , soil water
The article describes the ore bearance of three stages of reflected activation of the Kamchatka middle massif: Late Cretaceous, Eocene, and Miocene. In the first stage, gold mineralization of the gold-quartz and gold-sulfide-quartz formations was formed; in the second - sulfide platinoid-copper-nickel; in the third - gold-copper-molybdenum-porphyry. The relationship of gold, sulfide platinoid-copper-nickel and gold-copper-molybdenum-porphyry mineralization with certain igneous rock complexes - (Kola, Dukuk and Lavkin) is shown. The mining of nickel, copper from the Shanuch deposit and gold from placers has been noted.

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