论花岗质岩浆多重侵位及其多重成矿模型
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


On the Multiple Emplacement of the Granitic Magma and the Multiple Minerogenetic Models
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
  • |
  • 文章评论
    摘要:

    我国许多斑岩型和斑岩-矽卡岩型矿床具有“多位一体”特征,在区域上可构成矿床系列,在矿区则构戒矿床体系。本文强调这种多重成矿模型的普遍意义,提出花岗质岩浆的源岩、侵位和矿化的多重性是形成复杂多样的金属矿床的重要原因之一。重视和加强多重成矿模型研究,对于开拓找矿思路是十分有益的。

    Abstract:

    Many of the porphyry, porphyry-skarn and other hydrothermal ore deposits in Ch na are characterized by the"multi-type". They form deposit series regionally and deposit systems locally. With emphasis on universal significance of the multiple minerogenetie models, this paper points out that the multiplieity of the source rocks, emplacement and mineralization of the granitic magma is one of the important geneses of the complex and various mineral deposits. Thus, it is essential to study emphatically on the multiple minerogenetic models to developing the mineralization theories and extending the train of thoughts of the exploration.

    参考文献
    相似文献
    引证文献
引用本文

芮宗瑶,张洪涛,李 宁,等, 1991. 论花岗质岩浆多重侵位及其多重成矿模型[J]. 岩石矿物学杂志, 10(2):97~104.
Rui Zongyao Zhang Hongtao Li Ning Wang Longsheng, 1991. On the Multiple Emplacement of the Granitic Magma and the Multiple Minerogenetic Models[J]. Acta Petrologica et Mineralogica, 10(2): 97~104.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期:
文章二维码