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J4 ›› 1998, Vol. 6 ›› Issue (4): 1-7.

• 地质·矿床 •    下一篇

初论深部流体与成矿作用

杨金中1,沈远超1,赵玉灵2   

  1. 1.中国科学院地质研究所 北京 100029;
    2.长春科技大学 长春 130026
  • 收稿日期:1998-04-01 出版日期:1998-08-28 发布日期:2011-11-07
  • 作者简介:杨金中,男,1960 年出生,博士生,从事大地构造与成矿、成矿预测等研究。

DEEP-SEATED FLUID AND ITSMETALLOGENY

Yang Jinzhong1,Shen Yuanchao1,Zhao yuling2   

  1. 1.Institute of Geology,Chinese Academy of Sciences Beijing  100029;
    2.Chang chun University of Science and Technology  130026
  • Received:1998-04-01 Online:1998-08-28 Published:2011-11-07

摘要:

地壳乃至上地幔的流体运动与成矿作用的关系正日益受到国内外地质学家的关注,主要介绍深部流体的来源、分布及运移途径,对部分构造运动过程中的流体作用进行了探讨,并结合新疆北部金矿床的研究成果,认为流体作用不仅控制了成矿作用的进程,而且对构造运动具有明显的影响。

关键词: 深部流体, 成矿作用, 俯冲带

Abstract:

The relationship among deep-seated fluid movements,diagenesis and mineralization in the crust and the mantle is paid more attention to than whenever else in the past.The fluid has played a principal role during all kinds of geological process.This paper mainly reviews the formation,distribution and evolution of deep-seated,the function of fluid during geological process.Connected to the mineralization and metallogeny in Xinjiang,it is suggested that fluid study not only proclaims various geological process of the crust and even the deep part of the earth,but also systematically explains the relationship between formation and evolution of fluid and mineralization.

Key words: deep-seated fluid, metallogeny, subduction belt

中图分类号: 

  • P12/P618.51


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[1] 沈远超,曾庆栋,刘铁兵,谢宏远,李光明. 山东省金矿类型及找矿方向探讨[J]. J4, 1998, 6(3): 1-5.
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