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地质调查评价下的新疆地区铜矿床地质特征及成因

樊利强

世界有色金属Issue(2):99-101,3.
世界有色金属Issue(2):99-101,3.

地质调查评价下的新疆地区铜矿床地质特征及成因

Geological characteristics and genesis of copper deposits in Xinjiang region under geological survey evaluation

樊利强1

作者信息

  • 1. 新疆地质局乌鲁木齐地质大队,新疆 乌鲁木齐 830000
  • 折叠

摘要

Abstract

This article studies the geological characteristics and genesis of the copper deposit in Kongquegou area,Xinjiang.Combining the regional geological background,ore body characteristics,ore composition,and surrounding rock alteration characteristics,the formation process of the deposit is analyzed in depth.Through field geological surveys,core analysis,and mineralogical studies,the structural ore controlling characteristics,ore composition,and mineralization processes of the ore body were explored.The research results indicate that the Kongquegou copper deposit is a typical hydrothermal deposit,and mineralization is closely related to fault structures and magmatic hydrothermal activity.The phenomenon of surrounding rock alteration(such as sericitization and silicification)and the distribution pattern of ore bodies provide important indicators for mineral exploration.The research conclusion provides a theoretical basis for further mineral exploration in the region.

关键词

铜矿床/地质调查/孔雀沟铜矿床

Key words

copper deposit/Geological survey/Kongquegou copper deposit

分类

地质学

引用本文复制引用

樊利强..地质调查评价下的新疆地区铜矿床地质特征及成因[J].世界有色金属,2025,(2):99-101,3.

世界有色金属

1002-5065

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