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首页> 外文期刊>Journal of China University of Geosciences >Metallogeny of Shoshonite-Hosted Copper-gold Deposits in Middle-South Parts of Tancheng- Lujiang Deep Fault Zone and Its Vicinity, Eastern China
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Metallogeny of Shoshonite-Hosted Copper-gold Deposits in Middle-South Parts of Tancheng- Lujiang Deep Fault Zone and Its Vicinity, Eastern China

机译:中国东部Tan城-庐江深断裂带中南部部分白云母型铜金矿床的成矿作用

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摘要

The middle-south parts of Tancheng-Lujiang deep fault zone and its vicinity are an importan locality of Cu-Au deposits related to Mesozoic volcanic-subvolcanic magmatism in eastern china. According to their metallogenic features and ore-forming conditions, copper-gold deposits in this District are ascribed to two groups: the epithermal group which can be further divided into telluri- Um-gold type, quartz-adularia type and quartz-manganoansiderite type; the magmatic hydrother- Mal group which includes porphyry Cu-Au deposit, breccia pipe-porphyry type Au-Cu depsit and Skarn type Au-Cu deposit.
机译:Tan城—庐江深断裂带的中南部及其附近地区是我国东部中生代火山—次火山岩浆作用的重要部位。根据其成矿特征和成矿条件,该区铜金矿床可分为两类:超热组,可进一步分为碲-金-铀型,石英-金刚砂型和石英-锰铁矿型。岩浆水热-马尔组,包括斑岩型铜金矿床,角砾岩型斑岩型金铜矿床和矽卡岩型金铜矿床。

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