地质流体与构造运动

doi:10.11867/j.issn.1001-8166.1994.03.0024

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

地质流体与构造运动

陶于祥,谢鸿森

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

Institute of Geochemistry, Academic Sinica, Guiyang 550002

Received:1993-06-01 Revised:1993-10-25 Online:1994-05-01 Published:1994-05-01

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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。

关键词: 地质流体, 岩石应变, 裂隙, 中型构造

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).

Key words: Geologyfluids, Rock strain, Fractures, Mid-scale structures.

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