Tectonics and metallogeny of the Khakandzha ore district in the Okhotsk–Chukotka volcanic belt
- Autores: Yushmanov Y.1, Petrishchevsky A.1,2
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Afiliações:
- Institute of Complex Analysis of Regional Problems
- National Research Tomsk Polythechnical University
- Edição: Volume 10, Nº 5 (2016)
- Páginas: 337-350
- Seção: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211128
- DOI: https://doi.org/10.1134/S1819714016050055
- ID: 211128
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Resumo
The data on the structure, geodynamics, and metallogeny of the Khakandzha ore district in northwestern Okhotsk region are analyzed and the two main factors responsible for the localization of ore deposits are defined. The magmatic factor controls the confinement of the ore district to the tectono-magmatic structure of the central type (source of ore matter), which determines the concentric zoning patterns in the distribution of ore mineralization. The tectonic factor determines the confinement of the ore districts, deposits, and ore occurrences of the region to the meridional left-lateral shear structure, which controls the magma and fluid distribution. Local extension (transtension) in this structure against the background of general lateral compression (transpression) provided tectonic environments most favorable for ore accumulation.
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Sobre autores
Yu. Yushmanov
Institute of Complex Analysis of Regional Problems
Email: petris2010@mail.ru
Rússia, ul. Sholom Aleikhema 4, Birobidzhan, 697016
A. Petrishchevsky
Institute of Complex Analysis of Regional Problems; National Research Tomsk Polythechnical University
Autor responsável pela correspondência
Email: petris2010@mail.ru
Rússia, ul. Sholom Aleikhema 4, Birobidzhan, 697016; ul. Lenina 30, Tomsk, 634050