华北克拉通绿岩带型金成矿系统初析

翟裕生; 苗来成; 向运川; 邓军; 王建平

Volume 27 Issue 5

Sep. 2002

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Article Navigation > Earth Science > 2002 > 27(5): 522-531

ZHAI Yu-sheng, MIAO Lai-cheng, XIANG Yun-chuan, DENG Jun, WANG Jian-ping, 2002. Preliminary Discussion on Gold Ore-Forming System in Greenstone Belt-Type of North China Craton. Earth Science, 27(5): 522-531.

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Preliminary Discussion on Gold Ore-Forming System in Greenstone Belt-Type of North China Craton

1.
Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

Received Date: 2002-05-30
Publish Date: 2002-10-25

Abstract

Abstract

The greenstone belt type gold deposit in the North China craton (NCC), one of the most important deposit types in China, is the major source of gold productions and reserves. In terms of geodynamics, the NCC has experienced several tectonic stages ranging from the Middle and Upper Proterozoic divergent epicontinents, the Lower to Upper Paleozoic convergent epicontinents, to the Phanerozoic Mesozoic craton activation. This type of gold deposit, formed mainly in the craton activation stage, occurred in the transitional period from a compressive regime of late or post collision to an extension one. Gold mineralization occurred in a favorable regional geochemical setting (fairly high abundance of gold). Although these deposits were formed in different Phanerozoic periods, with the majority of these deposits in the Late Yanshanian, they share similar geological and geochemical features, and are spatially, temporally and genetically related to Phanerozoic granitic intrusions. Geochronological data suggest that gold mineralization is coeval with, or slightly postdates, the emplacement of the associated granites, probably indicating that gold mineralization is likely a product of the late stage of tectono magmatism. Therefore, the major gold deposits in the NCC can be considered as a single metallogenic system, i.e., hydrothermal metallogenic system related to granitic magmatism in greenstone belts.
- North China craton,
- greenstone belt,
- gold deposit,
- metallogenic system

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References(50)

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