摘要
构造(应力)和流体是许多地质作用过程中发挥重要作用的两个基本因素。构造作用与流体的关系十分密切,两者相互影响、相互作用的关系称为构造—流体作用。压溶作用、流体致裂作用和裂隙闭合作用等是重要类型的构造—流体作用。本文阐述了它们的发育机理和地质意义。深入研究这些构造—流体作用及其效应,可为重塑地质历史和过程的研究提供重要的“化石”材料。
The structure/stress and fluids are two fundamental factors that play a very important role in various geological processes. The structure or tectonism is closely related to fluids. There are many kinds of structure-fluid interactions in nature, among which the pressure solution, the fluid-induced cracking, and the crack closing are the most important ones during the geological processes. The present paper deals with the development mechanisms and the geological implications of the above three structure-fluid interactions. It is pointed out that the study of the structure-fluid interaction and its geological effects can provide useful 'fossil' data for us geologists to reconstruct and understand the geological history and geological processes.
出处
《地质论评》
CAS
CSCD
北大核心
2002年第5期495-504,共10页
Geological Review
基金
国家自然科学基金项目(编号 40002021)
教育部留学回国科研启动基金