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    时俊峰. 小西南岔金铜矿床地质特征及成因机制[J]. 地质与资源, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
    引用本文: 时俊峰. 小西南岔金铜矿床地质特征及成因机制[J]. 地质与资源, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
    shu
    Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
    Citation: Shi Junfeng. GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT[J]. Geology and Resources, 1998, 7(4): 274-280. DOI: 10.13686/j.cnki.dzyzy.1998.04.005
    shu

    小西南岔金铜矿床地质特征及成因机制

    GEOLOGICAL CHARACTERISTICS AND MINEROGENEIC MECHANISM OF THE XIAOXINANCHA GOLD COPPER DEPOSIT

      摘要
    • 摘要: 小西南岔金铜矿床产于下古生界五道沟群与华力西晚期闪长岩内接触带中.矿化类型为含金石英硫化物脉型及密集细脉型.矿体受近S-N向断裂、NW向断裂及裂隙构造带控制，矿床成因类型为岩浆热液型.

       

      Abstract: Xiaoxinancha gold-copper deposit occurs in the contact between the Late Variscan diorite and Lower Palaeozoic Wudaoguo group The mineralizing types include gold bearing quartz-sulfide veins and concentrated veinlets The ore bodies are controlled by S-N-and NW-trending faults or fractures The deposit is magmatic hydrothermal origin

       

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