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中文摘要: 通过对获各琦铜矿矿体特征、地球化学特征、以及其它控矿因素等方面的分析得出，该矿区铜矿体主要赋存在狼山群第二岩组中段的条带状石英岩中，并且构造控制了矿床的展布；地层控制了矿体的规模；岩性控制了矿体的种类和产状。因此，获各琦铜矿是典型的以沉积岩为容矿岩石的喷流沉积矿床，后经变质及岩浆作用改造形成。本文进一步了解获各琦铜矿的成矿规律，为矿山的深部和外围探矿做准备。
Abstract:Through the analysis of copper orebody characteristics, geochemistry and other controlling factors of the huogeqi copper mine, it was realized that mine copper orebody mainly occurs in the banded quartzite in the middle of second group of Langshan mountain formation, where the structures control the deposit distribution, the stratum controls the size of orebody, the lithology controls the type and occurrence of the ore bodies. Therefore, it was a typical SEDEX deposits for sedimentary rock as the host rock, and it was transformed by metamorphism or magmatism. The purpose of this paper was to further understand the metallogenic regularity of the huogeqi copper mine for deep and peripheral exploration.
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彭福军,代建清,张升源.获各琦铜矿的铜矿体特征及赋存规律[J].有色金属（矿山部分）,2011,63(2):28-30.
PENG Fujun,DAI Jianqing,ZHANG Shengyuan.The Characteristics and occurrence regularity of copper orebody in Huogeqi Copper Mine[J].NONFERROUS METALS(Mining Section),2011,63(2):28-30.
彭福军,代建清,张升源.获各琦铜矿的铜矿体特征及赋存规律[J].有色金属（矿山部分）,2011,63(2):28-30.
PENG Fujun,DAI Jianqing,ZHANG Shengyuan.The Characteristics and occurrence regularity of copper orebody in Huogeqi Copper Mine[J].NONFERROUS METALS(Mining Section),2011,63(2):28-30.
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