Geological characteristics and genesis of Shatanjiao ore field in Tongling ore district,Anhui
Han Chang-shen
Abstract
Han Chang-shen
Abstract
The Shatanjiao polymetallic ore field,located in the eastern of Tongling uplift district in the Middle-Lower Yangtze River Valley metallogenic belt,is a significant potential mineralization area. There are thirteen deposits in the area,including a super-large deposit called Yaojialing,and some other small deposits called Shatanjiao,Zhujiachong,Daiyaoshan,Fengxingshan,Xiaogongshan and so on.The major types of the deposit are medium-low hydrothermal deposits and skarn type deposits. Mineralization assemblages are mainly composed of zinc-gold-copper polymetallic elements.Shatanjiao and Yaojialing intrusive rocks are both important related rocks for mineralization,and the dominant ore-forming related formations are Carbonic-Permian carbonatite rocks.The metallogenetic process of Shatanjiao ore field is a part of Yanshannian mineralization in Tongling ore district.
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The Shatanjiao polymetallic ore field,located in the eastern of Tongling uplift district in the Middle-Lower Yangtze River Valley metallogenic belt,is a significant potential mineralization area. There are thirteen deposits in the area,including a super-large deposit called Yaojialing,and some other small deposits called Shatanjiao,Zhujiachong,Daiyaoshan,Fengxingshan,Xiaogongshan and so on.The major types of the deposit are medium-low hydrothermal deposits and skarn type deposits. Mineralization assemblages are mainly composed of zinc-gold-copper polymetallic elements.Shatanjiao and Yaojialing intrusive rocks are both important related rocks for mineralization,and the dominant ore-forming related formations are Carbonic-Permian carbonatite rocks.The metallogenetic process of Shatanjiao ore field is a part of Yanshannian mineralization in Tongling ore district.
Key concepts: Mineralization (soil science), Geology, Skarn, Geochemistry, Carbonatite, Permian, Ore genesis, Polymetallic replacement deposit