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浩斯台铜银多金属矿地质特征及成矿规律研究

隋海涛 张立松 王晓东

世界有色金属Issue(2):65-67,3.
世界有色金属Issue(2):65-67,3.

浩斯台铜银多金属矿地质特征及成矿规律研究

Study on the Geological Characteristics and Metallogenic Regularity of the Haositai Copper-Silver Polymetallic Deposit

隋海涛 1张立松 1王晓东2

作者信息

  • 1. 内蒙古第十地质矿产勘查开发有限责任公司,内蒙古 赤峰 024000
  • 2. 内蒙古地质勘查有限责任公司,内蒙古 呼和浩特 010000
  • 折叠

摘要

Abstract

Houstai copper-silver polymetallic mine in Zhalut Banner is located in the central and southern section of the Greater Hinggan Mountains,with complex geological background,and the formation of pre-Mesozoic fold base and the process of middle and Cenozoic structure-magma activation.Mainly exposed carboniferous and Jurassic strata,the tectonic line is mainly north and east,and the intrusive rocks are mainly medium acid.Mineralization types are rich,the development of copper,lead,zinc and other metal ore bodies,mineralization is related to the early Triassic granodiorite.The geophysical and chemical anomaly shows the mineralization potential and the prospect of further prospecting.

关键词

铜银多金属矿/成矿规律/地质特征/内蒙古浩斯台

Key words

Copper-silver polymetallic ore/metallogenic regularity/geological characteristics/Haositai,Inner Mongolia

分类

天文与地球科学

引用本文复制引用

隋海涛,张立松,王晓东..浩斯台铜银多金属矿地质特征及成矿规律研究[J].世界有色金属,2025,(2):65-67,3.

世界有色金属

1002-5065

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