最大左行走滑活动时期当在中晚三叠世。
The forming age of maximum sinistral strike-slip occurred in Middle-Late Triassic.
由于北东向断层的左行走滑，在丰州一带生成拉分盆地。
Resulting from the sinistral displacement of the NE-trending fault, there is a pull-apart basin in the Feng Zhou area.
新近纪阿尔金断裂在左行走滑的大背景下经历了一个陆内的拉张—挤压旋回。
The Altun fault experienced an intracontinental cycle of extension-compression during Neogene in a background of sinistral strike-slipping.
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