山东省邹平铜矿17号矿体矿床成因
DOI:
作者:
作者单位:

作者简介:

通讯作者:

基金项目:


Discussion on the Origin of No.17 Copper Orebody of Zouping Cooper Deposit in Shandong Province
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
    摘要:

    邹平铜矿17号矿体是高中温热液矿床并严格受隐爆角砾岩筒控制,而非伟晶岩型矿床,已被海内外众多同行所认可。该文在勘查结合坑道观测的基础上,通过深入研究和分析对比,进一步证实并坚定了对矿床成因的认识,并澄清了一些模糊看法及无根据的推测。

    Abstract:

    No.17 orebody of Zouping copper deposit is a highmedium thermal deposit. It is strictly controlled by cryptoexplosive breccia rock pipe. It does not belong to pegmatite deposit which has been recognized by many colleagues in China and abroad. On the basis of exploration and tunnel observation, through study, analysis and contrast, the origin of this deposit has been determined, and some fuzzy thoughts and guess have been identified as well.

    参考文献
    相似文献
    引证文献
引用本文

赵祉友,高伯兴,张相峰,徐勇,孟祥进,荣丹文.山东省邹平铜矿17号矿体矿床成因[J].山东国土资源,2012,28(9):

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期: