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内蒙古克什克腾旗哈尔楚鲁图银多金属矿区矿床成因及找矿标志

The Genesis and Prospecting Mark of the Halchulutu Silver Polymetallic Deposit in Keshiketengqi,Inner Mongolia

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【作者】 张艳军房晓红

【Author】 ZHANG Yan-jun;FANG Xiao-hong;Taiyuan University of Technology;3rd Geological Exploration Institute,China Metallurgical Geology Bureau;

【机构】 太原理工大学中国冶金地质总局第三地质勘查院

【摘要】 通过对内蒙古克什克腾旗哈尔楚鲁图银多金属矿区成矿地质背景、矿床(体)地质特征、矿物组合类型等进行分析研究,认为区内矿体严格受北西向构造控制,矿床成因类型为岩浆期后中-低温热液充填式脉状铅锌多金属矿床,并提出本区的找矿标志,以指导矿区勘查工作。

【Abstract】 This paper analyzes and studies the metallogenic geological background,the geological features and the types of mineral associations in the Halchulutu silver polymetallic ore district of Heshiketengqi,Inner Mongolia. It is believed that the orebodies in the area are strictly influenced by the northwestern structure. Control,the type of genetic deposit is a postmagmatic low-temperature hydrothermal-filled pulsed lead-zinc polymetallic deposit in the magmatic stage,and the prospecting signs in this area are proposed to guide the exploration work in the mining area.

  • 【分类号】P618.2
  • 【被引频次】2
  • 【下载频次】43
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