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川西北银厂金矿床地球化学特征及成因探讨

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熊观, 段威, 唐文春, 杨贵兵, 王焕国, 黄健. 2020. 川西北银厂金矿床地球化学特征及成因探讨. 西北地质, 53(4): 86-98. doi: 10.19751/j.cnki.61-1149/p.2020.04.008
引用本文: 熊观, 段威, 唐文春, 杨贵兵, 王焕国, 黄健. 2020. 川西北银厂金矿床地球化学特征及成因探讨. 西北地质, 53(4): 86-98. doi: 10.19751/j.cnki.61-1149/p.2020.04.008
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XIONG Guan, DUAN Wei, TANG Wenchun, YANG Guibing, WANG Huanguo, HUANG Jian. 2020. On the Geochemical Characteristics and Genesis of the Yinchang Gold Deposit in Northwestern Sichuan Province. Northwestern Geology, 53(4): 86-98. doi: 10.19751/j.cnki.61-1149/p.2020.04.008
Citation: XIONG Guan, DUAN Wei, TANG Wenchun, YANG Guibing, WANG Huanguo, HUANG Jian. 2020. On the Geochemical Characteristics and Genesis of the Yinchang Gold Deposit in Northwestern Sichuan Province. Northwestern Geology, 53(4): 86-98. doi: 10.19751/j.cnki.61-1149/p.2020.04.008
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川西北银厂金矿床地球化学特征及成因探讨

  • 1. 四川省地质矿产勘查开发局化探队, 四川 德阳 618000;

  • 2. 四川省深地地质勘查有限公司, 四川 德阳 618000

  • 基金项目:

    四川省地矿局2018年度局科技研发计划项目“四川平武银厂金矿深部地质找矿研究”（2018-5）

详细信息
    作者简介: 熊观(1984-),男,湖南省华容县,高级工程师,硕士,从事地质调查、矿产勘查及研究工作。E-mail:18771145@qq.com

  • 中图分类号: P618.51

On the Geochemical Characteristics and Genesis of the Yinchang Gold Deposit in Northwestern Sichuan Province

  • 1. Sichuan Prospecting and Exploiting Bureau and Geochemical Exploration Team of Geology and Mineral, Deyang 618000, Sichuan, China;

  • 2. Sichuan Deep Resource Geological Exploration Co., Ltd., Deyang 618000, Sichuan, China

    摘要
  • 为探讨银厂金矿床的地球化学特征及成因，测试了石英包裹体均一温度、盐度和S-H-O同位素组成。研究表明，成矿物质来源主要是三叠系杂谷脑组浅变质碎屑岩，成矿流体为深源流体与变质水的混合热流体，成矿温度为中低温。矿床成因类型为断裂控制的中低温热液型金矿床。
    This paper measured the homogenization temperature, salinity and S-H-O isotopic compositions of the quartz inclusions in order to study the geochemical characteristics and genesis of the Yinchang gold deposit. The results show that the ore-forming source is mainly from the epimetamorphic clastic rocks of Triassic Zagunao Group. The metallogenic fluid is a mixture of juvenile fluid with metamorphic water. The metallogenic temperature is low or medium. The genetic type of Yinchang gold deposit is a low-or-medium temperature hydrothermal deposit controlled by fracture.
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收稿日期:  2020-03-16
修回日期:  2020-08-14

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