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2007•Yunnan GeologyRequires access

THE METALLOGENETIC MODEL OF BAOXINGCHANG AU DEPOSIT IN MIDU,YUNNAN

HE Zheng-zhong

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Abstract

The geological structure of Baoxingchang orefield is complicated and the metallogenetic condition is advantageous.The northeastward Xiangshui fault zone in this area is the main rock-control and ore-control structure.There are 3 types of Au deposit,which are formed separately in the porphyry metallogenetic period,hydrothermal metallogenetic period,epigenetic metallogenetic period and have their corresponding metalloge-netic models.

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The geological structure of Baoxingchang orefield is complicated and the metallogenetic condition is advantageous.The northeastward Xiangshui fault zone in this area is the main rock-control and ore-control structure.There are 3 types of Au deposit,which are formed separately in the porphyry metallogenetic period,hydrothermal metallogenetic period,epigenetic metallogenetic period and have their corresponding metalloge-netic models.

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Available abstract

The geological structure of Baoxingchang orefield is complicated and the metallogenetic condition is advantageous.The northeastward Xiangshui fault zone in this area is the main rock-control and ore-control structure.There are 3 types of Au deposit,which are formed separately in the porphyry metallogenetic period,hydrothermal metallogenetic period,epigenetic metallogenetic period and have their corresponding metalloge-netic models.

Key concepts: Hydrothermal circulation, Geology, Period (music), Fault (geology), Geochemistry, Mineralogy, Mining engineering, Paleontology

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