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甘肃天水后驮阳金矿床成因分析及找矿方向

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后驮阳金矿床位于西秦岭东段,矿化类型为热液脉状和构造蚀变岩型.综合研究认为,矿床整体受下古生界丹凤群地层-北东东向断裂构造-闪长玢岩等联合控制,成矿时代为印支中晚期,成因类型为与岩浆作用有关的金矿床(IRGD型).在此基础上,总结了闪长玢岩、北东东向断裂、断裂构造交汇部位以及岩体中深部等找矿方向.
Genetic analysis and prospecting direction of the Houtuoyang gold deposit in Tianshui,Gansu Province
The Houtuoyang gold deposit is located in the eastern section of the Western Qinling Mountains,with mineralization types of hydrothermal vein and tectonic altered rock.According to comprehensive research,the overall ore deposit is controlled by the Lower Paleozoic Danfeng Group strata,northeast trending fault structures,diorite porphyry,and other factors.The mineralization period is in the middle to late Indosinian period,and the genetic type is related to magmatic activity of the gold deposit(IRGD type).On this basis,the prospecting directions for diorite porphyry,northeast trending faults,intersection of fault structures,and deep rock masses were summarized.

HoutuoyangGold minesDiorite porphyriteExploration direction

张羿生、刘文江、望开磊、汪世勇

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甘肃省天水李子金矿有限公司,甘肃 天水 741004

后驮阳 金矿 闪长玢岩 找矿方向

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(3)
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