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东昆仑尕牙河东沟铜镍矿床地质特征及找矿前景分析

Geological characteristics and prospecting potentials analysis in Gayahedonggou Copper-Nickel Deposit,East Kunlun

  • 摘要: 尕牙河东沟铜镍矿床位于东昆仑造山带,临近昆中断裂,成矿地质条件优越。矿区内共发现4个镁铁质—超镁铁质岩体,岩体主要岩性为辉橄岩、辉石岩、辉长岩、辉石橄榄岩、橄榄岩、橄榄透闪石岩、斜长岩等。在Ⅰ、Ⅱ、Ⅳ镁铁质—超镁铁质岩体中均发现了铜镍矿体,赋矿岩性主要为橄榄岩、辉石岩,其次为辉长岩。通过分析矿区地质、地球化学和地球物理特征,结合与同一造山带内的典型矿床对比,认为具有寻找岩浆铜镍矿体的有利条件,具有较好的找矿前景。

     

    Abstract: Gayahedonggou Copper-Nickel Deposit is located in East Kunlun orogenic belt adjacent to Great Middle Kunlun Fracture and bears favorable ore-forming geological conditions.4 magnesian ferrous-super magnesian ferrous rock mass bodies are found in the district that mainly include peridotite,pyroxenite,gabbro,pyroxene peridotite,peridotite,peridotite tremolite and anorthosite.In magnesian ferrous-super magnesian ferrous rock mass bodies Ⅰ,Ⅱand Ⅳ,copper-nickel ore bodies are found,peridotite and pyroxenite mainly included followed by peridotite.Based on the geological,geochemical and geophysical characteristics analysis,and the comparison between the typical deposits from the same orogenic belt,it is considered that the district has favorable conditions for magmatic copper-nickel ore bodies prospecting and great prospecting potentials.

     

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