The fault is of brittle type in the shallow tectonic level of the earth's crust. The main deformational mechanism is cataclasis.
The kinematic and dynamic features of the Enshi fault in the 3 main deformational phases are analyzed by means of the striations on fault planes, conjugate joints and microstructure in fault zone.
The time and space distribution of the Jurassic-Cretaceous basins and their deformational characteristics are related to Yanshan-Qikou-Xingang buried faulted zone and the Mesozoic Cangdong faulted zone.
Influence of viscosity of ductile substrate on deformational features of fold-thrust belts: insights from physical modeling
The deformational dynamics is controlled by the compressional settings which are caused by the minor-angle oblique subduction of the Izanagi Plate and the continent-to-continent collision betneen the Yangtze Plate and the North China Plate.
The paper discusses theoretically how to obtain the stress of flange deformational zone.
