假熔岩和碎裂岩类断层岩的存在，可作为古地震事件的可能证据。
The existences of pseudotachylite and cataclasite types of fault rocks can be regarded as the potential evidences for seismic events.
大量资料表明，微观分析是探讨松散沉积物中断层和古地震事件的行之有效的方法。
Recently, a lot of data have shown that microscopic analysis is an effective approach to the identification of obscured faults and paleo-earthquake event in soft sediments.
上述结果表明，微观分析是探讨松散沉积物中形迹不明断层和古地震事件的有效手段。
All the results show that microscopic analysis is an effective method for identifying obscured fault and paleo-seismic event in soft sediments.
在时间上，古地震事件的分布是不均匀的，具有丛集的特征；在空间上，具有西段或中东段（中段）来回迁移的特征。
The paleoevents are characterized by clustering in time and migrated back and forth from the west segment to middle - east segment.
在时间上，古地震事件的分布是不均匀的，具有丛集的特征；在空间上，具有西段或中东段（中段）来回迁移的特征。
The paleoevents are characterized by clustering in time and migrated back and forth from the west segment to middle - east segment.
应用推荐