Porphyry Cu-Mo deposits and geodynamic settings, Siberia, Mongolia

被引：0

作者：

Berzina, AP ^{[1
]}

Sotnikov, VI ^{[1
]}

Berzina, AN ^{[1
]}

机构：

[1] United Inst Geol Geophys & Mineral, Novosibirsk, Russia

来源：

MINERAL DEPOSITS: PROCESSES TO PROCESSING, VOLS 1 AND 2 | 1999年

关键词：

D O I：

暂无

中图分类号：

P57 [矿物学];

学科分类号：

070901 ;

摘要：

The Siberian and Mongolian porphyry Cu-Mo deposits are confined to early Paleozoic, late Paleozoic and Mesozoic magmatic belts including magmatic complexes of various geodynamic settings (of subduction, collision and rifting nature). According to geological and isotopic data, ore-bearing porphyries were formed during rifting, but inherited petrogeochemical features of the preceding collision and subduction magmatism to a certain extent. The Siberian and Mongolian porphyry Cu-Mo deposits seem to be related to long-lived magmatic super-systems which were active in different geodynamic environments (from subduction and collision to rifting).

引用

页码：317 / 320

页数：4

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