Any place within the fault zone could have breakage . 斷層帶內(nèi)的任何地方都會有破裂。
The gouge of the fault zone may extend to depths of some kilometers . 斷層區(qū)的斷層泥可能伸展到若干公里的深度。
Variations in rock type and structure in the fault zone would entail variations in slippage rate along the trace . 斷層區(qū)的巖石類型和構(gòu)造的不同將會引起沿斷痕滑動的速率的變化。
Along fault zones in particular, displacement may occur by slow, secular, differential slippage as well as by sudden rupture . 特別是沿著斷層區(qū),位移既可能以緩慢的,持久的、有差異的滑動發(fā)生,也可能以突然破裂發(fā)生。
Recent activity of chihe segment of tanlu fault zone 郯廬斷裂帶池河段的新活動