Tectonics and metallogeny of the Khakandzha ore district in the Okhotsk–Chukotka volcanic belt; Russian Journal of Pacific Geology; Vol. 10, iss. 5

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Parent link:Russian Journal of Pacific Geology
Vol. 10, iss. 5.— 2016.— [P. 337–350]
Tác giả chính: Yushmanov Yu. P. Yury Petrovich
Tác giả của công ty: Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии
Tác giả khác: Petrishchevsky A. M. Alexander Mitrofanovich
Tóm tắt:Title screen
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.
Режим доступа: по договору с организацией-держателем ресурса
Ngôn ngữ:Tiếng Anh
Được phát hành: 2016
Những chủ đề:
Truy cập trực tuyến:http://dx.doi.org/10.1134/S1819714016050055
Định dạng: Điện tử Chương của sách
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=651167

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