在地壳不同深室中,与断层活动伴随的剪应力大小是个重要的悬而未决的问题。从不同的角室来解决这个问题时出现了矛盾的意见和模棱两可的观点。例如,在圣安德列斯断层出现的高热流异常,就被假没为剪应力不能超过几百巴。另一方面,也有反对这个论点的意见,由于地下水流动,传导热量而引起显著的异常,这也是可能的。由岩石实验资料所决定的摩 In different deep crusts, the magnitude of shear stress associated with fault activity is an important and outstanding issue. There have been conflicting opinions and ambiguities in resolving this issue from different angles. For example, the high heat flow anomalies that occur in the San Andres Fault should not exceed a few hundred barrels of shear stress. On the other hand, there are also arguments against this argument, which are also possible due to the significant anomalies caused by the flow of groundwater and the conduction of heat. The friction determined by the rock experimental data