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紫金山金铜矿床东南矿段蓝辉铜矿特征及成因

Characteristics and genesis of digenites in southeast mining segment of Zijinshan Au−Cu Deposit

  • 摘要: 紫金山金铜矿床具有保存较完整的浅成低温热液−斑岩铜金多金属成矿系统。通过详细的岩石学及岩相学工作,总结了紫金山金铜矿床东南矿段蓝辉铜矿的矿物组合及结构特征。根据其宏观、微观特征,划分出了3种类型蓝辉铜矿,分别为浸染状(Ⅰ型)蓝辉铜矿、硫化物脉状(Ⅱ型)蓝辉铜矿和蚀变脉状(Ⅲ型)蓝辉铜矿,结合前人资料划分了紫金山金铜矿床东南矿段主要金属矿物的生成顺序。结合金属硫化物矿物组合及与蚀变之间的关系,初步认为3种蓝辉铜矿均为与热液作用相关的原生蓝辉铜矿。其中,Ⅰ型蓝辉铜矿与斑岩成矿系统有关,Ⅱ型和Ⅲ型蓝辉铜矿与浅成低温热液成矿系统有关。紫金山金铜矿床东南矿段蓝辉铜矿是斑岩成矿系统向浅成低温热液成矿系统过渡带的产物。

     

    Abstract: The Zijinshan Au−Cu Deposit is a well-preserved epithermal-porphyry Cu−Au polymetallic metallogenic system. Through detailed petrological and petrographic studies, the mineral assemblages and structural features of digenite in the southeast mining segment of the Zijinshan Au−Cu deposit were summarized. Based on their macro and micro characteristics, 3 types of digenite were identified: typeⅠdigenite with disseminated textures, type Ⅱ digenite with sulfide vein textures, and type Ⅲ digenite with alteration vein textures. In conjunction with previous data, the sequence of formation of the main metallic minerals in the southeast mining segment of the Zijinshan Au−Cu Deposit was established. Based on the combination of metallic sulfide minerals and their relationship with alteration, it is preliminarily concluded that all 3 types of digenite are primary digenites associated with hydrothermal action. Type Ⅰ digenite is related to the porphyry metallogenic system, while types Ⅱ and Ⅲ digenite are associated with epithermal metallogenic systems. The digenite in the southeast mining segment of the Zijinshan Au−Cu Deposit is a product of the transition zone from the porphyry metallogenic system to the epithermal metallogenic system.

     

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