| 注册
首页|期刊导航|地质与勘探|贵池铜山铜矿床成因探讨

贵池铜山铜矿床成因探讨

俞沧海

地质与勘探2001,Vol.37Issue(2):12-16,5.
地质与勘探2001,Vol.37Issue(2):12-16,5.

贵池铜山铜矿床成因探讨

STUDY ON THE GENESIS OF TONGSHAN COPPER ORE DEPOSIT IN GUICHI

俞沧海1

作者信息

  • 1. 铜陵有色公司技术中心,
  • 折叠

摘要

Abstract

The mineralization of Tongshan copper ore deposit can dividedinto the stratiform pyrite-type,breccia-type,skarn-type and prophyry-type. Control factors of mineralization are strata, magmatites and structure.Interformatinal faults and contract zone are mainly including ore structures. The study on the data of lead,sulfur,hydrogene,oxygen isotopesand minerogenetic temperature shows that the ore-forming materials and thermal fluid are mainly from the Tongshan rock body. The genetic type of ore deposit is strata-bound skarn-type copper ore deposit.

关键词

铜山/控矿因素/容矿构造/层控夕卡岩型铜矿床

分类

天文与地球科学

引用本文复制引用

俞沧海..贵池铜山铜矿床成因探讨[J].地质与勘探,2001,37(2):12-16,5.

地质与勘探

OA北大核心CSCD

0495-5331

访问量0
|
下载量0
段落导航相关论文