地球科学进展 ›› 1994, Vol. 9 ›› Issue (3): 24 -29. doi: 10.11867/j.issn.1001-8166.1994.03.0024

干旱气候变化与可持续发展 上一篇    下一篇

地质流体与构造运动
陶于祥,谢鸿森   
  1. 中国科学院地球化学研究所  贵阳 550002
  • 收稿日期:1993-06-01 修回日期:1993-10-25 出版日期:1994-05-01
  • 通讯作者: 陶于祥

GEOLOGY FLUIDS AND STRUCTURE MOVEMENT

Tao Yuxiang, Xie Hongsen   

  1. Institute of Geochemistry, Academic Sinica, Guiyang  550002
  • Received:1993-06-01 Revised:1993-10-25 Online:1994-05-01 Published:1994-05-01

运用大量的研究成果,综述了地质流体与岩石应变、微观裂隙开合,宏观(中等规模)褶皱、断裂的相互关系。并指出今后尚须加强中型构造运动过程中流体动力学基础理论、差异应力作用下水岩地球化学及其模拟实验、流体与灾害构造(泥石流、滑坡等)的关系等方面的研究。

This paper utilizes a large number of study results to explicate the relationship among geology fluids, rock strain, the growing and healing of micro-fractures, microscopic structures(folds, faults). The author points out: In the future, it is necessary to enhance the study on. The basic theory of fluids Kinetics in structure movement(Mid-Scale); Water-Rock geochemistry on the condition of differential stress and the study of their imitating experiment; The relationship between fluids and disastrous structures(soil flow, landslip).

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