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一、引言通过天然变形岩石的岩组分析,恢复岩石变形时的应力状态,结合地质观察,确定构造运动的来向和性质(较小的区域內),对构造地质学、矿田构造学和岩石学研究都有裨益。从岩石的实验变形出发,在给定的应力条件下研究变形岩石的组构变化,作为天然变形岩石组构分析的依据,也是不可缺少的一部分。近年来,不少地质学者愈来愈注意到天然变形的碳酸盐岩石的岩组学工作。到目前为止,对碳酸盐岩石(如变质白云岩)的岩组分析和动力学解释有两种情况。
I. INTRODUCTION Through the analysis of the rock group of the natural deformed rock and the restoration of the stress state during the deformation of the rock, combined with the geological observation, the orientation and the nature of the tectonic movement (within a small area) are confirmed. The tectonics of the tectono-geology, Petrology research has benefits. Starting from experimental deformation of rock, it is also an indispensable part to study the change of the structure of deformed rock under the given stress as the basis for the analysis of the structure of natural deformed rock. In recent years, many geologists have paid more and more attention to the petrography of naturally deformed carbonate rocks. So far, there have been two cases of petrophysical analysis and kinetic interpretation of carbonate rocks (such as metamorphic dolomites).