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黑刺沟金矿床成因特征探讨
引用本文:谢,群.黑刺沟金矿床成因特征探讨[J].甘肃地质学报,2003,12(2):67-72.
作者姓名:  
作者单位:甘肃省地矿局第二地勘院,甘肃省地矿局第二地勘院 甘肃兰州 730020,甘肃兰州 730020
摘    要:黑刺沟金矿位于秦祁昆地槽褶皱系南祁连地向斜构造带的西段。矿床赋存于断裂破碎带中,属构造蚀变岩型金矿床,受NW向断裂构造控制。矿床的主要控矿因素是构造,地层为成矿提供了主要物源,岩浆活动提供了部分流体及热动力,构造破碎带为成矿提供了空间。

关 键 词:黑刺沟金矿床  成因特征  成矿模式

DISCUSSION ON THE GENETIC CHARACTERISTICS OF HEICIGOU GOLD DEPOSIT
XIE Qun.DISCUSSION ON THE GENETIC CHARACTERISTICS OF HEICIGOU GOLD DEPOSIT[J].Acta Geologica Gansu,2003,12(2):67-72.
Authors:XIE Qun
Institution:No.2 Geology and Mineral Exploration Team, Gansu Provincial Bureau of Geology and Mineral Exploration and Development,Lanzhou 730020,China
Abstract:Heicigou gold deposit is regionally located at the western section of the southern Qilian geosyncline of Qinling-Qilian-Kunlunshan mountain fold system. The deposit is hosted in a faulted fracture zone and belongs to tectono-altered type gold deposit. Structures are the main ore- controlling factors, strata provided main materials for ore-forming, magmatic activity provided thermal liquid and thermal dynamic power and tecto-fracture zone served as space for ore material positioning.
Keywords:Heicigou gold deposit  Genetic characteristics  Metallogenic model  
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