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胶东焦家金矿床钾长石成因及成矿意义

覃祚焕 魏超 梁文飞 张良

山东国土资源Issue(4):36-40,5.
山东国土资源Issue(4):36-40,5.

胶东焦家金矿床钾长石成因及成矿意义

覃祚焕 1魏超 1梁文飞 1张良1

作者信息

  • 1. 中国地质大学,地球科学与资源学院,北京 100083
  • 折叠

摘要

Abstract

Jiaojia gold deposit belongs to altered rock type gold deposit,which has extensive wall rock al-teration.It is one of the biggest gold deposit in reserves.Occurrence and chemical composition of the K feldspar in the alteration rock have been analyzed and studied,and compared with the K feldspar in the non alterated Linglong rock bodies.Three genetic types of K feldspar occurred in Jiaojia gold deposit, including native K feldspar (magmatic origin),hydrothermal K feldspar of high temperature and hydro-thermal K feldspar of low temperature.Finally,combining with previous research,the formation and its mineralization significance of the hydrothermal K feldspar have been discussed.

关键词

围岩蚀变/热液钾长石/成矿意义/焦家金矿/胶东地区

Key words

Rock alteration/hydrothermal K feldspar/ore forming significance/Jiaojia gold deposit/Jiaodong area

分类

天文与地球科学

引用本文复制引用

覃祚焕,魏超,梁文飞,张良..胶东焦家金矿床钾长石成因及成矿意义[J].山东国土资源,2014,(4):36-40,5.

基金项目

国家大学生创新性实验计划项目 ()

山东国土资源

1672-6979

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