论文部分内容阅读
岩石破裂中的“里德尔切变”(Riedel Shear),是地质构造研究中常见的违反岩石破裂准则理论的逆反现象。文中侧重从应力应变理论的角度讨论了这一构造模式形成的机理,并结合典型构造实例对其进行了系统分析。
The “Riedel Shear” in the rock rupture is a common reversal phenomenon in the study of geological structures in violation of rock fracture criteria. In this paper, the mechanism of the formation of this structural model is discussed from the perspective of stress-strain theory, and it is systematically analyzed with typical structural examples.