The acceleration anomalies are mainly concentrated in adjusting unit in earthquake generating area or active segment of the fault.
加速异常主要集中在孕震区的调整单元或断层活动地段。
Strong earthquakes occurred mainly along the youngest and the most intensively active segment of the fault since the Holocene.
强震主要发生在全新世以来断裂的最新和最强烈的活动段上。
Each segment has a distinctive difference of its own in fault geometry, associated structures, active age and the sedimentation control etc.
各分段断层的结构、形态、伴生构造、活动时间及对沉积作用的控制等都存在较明显差异。
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