地震动力学过程最强烈地发生于活动不均匀层范围内,从地震学观点来看,位错过程扩展具有本质意义,其含义就是断块沿“原始”断裂或构造层之间的界面位移。前面已指出,现代位错过程伴随着岩石物理性质、各种地球物理场、流体动态和其他现象以及地壳内构造不均匀性几何尺度的异常 Seismic dynamics process occurs most intensely in the range of active heterogeneity. From a seismological point of view, the extension of dislocation process is of intrinsic significance. The implication of this is that the fault blocks displace along the “original” fault or interface between structural layers. It has been previously pointed out that modern dislocation processes are accompanied by rock physical properties, various geophysical fields, fluid dynamics and other phenomena as well as geometric anomalies of structural inhomogeneities within the crust