根据显微构造测定岩石中的古应力是Goetze(1975)最近提出的一种方法。然而,在一些情况下,显微构造并不反映出原始的变形状态。的确,必须采用最新的和最精确的实验来批判性地讨论“地质压力计”的问题,以便确定该“压力计”可靠到什么程度,并且根 The determination of paleo-stresses in rocks based on microstructures is a recently proposed method by Goetze (1975). However, in some cases, the microscopic structure does not reflect the original deformation state. Indeed, the latest and most rigorous experiments must be used to critically discuss the issue of “geostatistics” in order to determine to what extent the “gauge” is reliable, and the root