The Altun fault experienced an intracontinental cycle of extension-compression during Neogene in a background of sinistral strike-slipping.
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。
This study is a basis on revealing the tectonic evolution and active pattern, deducing the strike-slipping history and forecasting the future behavior of a strike-slip fault.
这一研究是揭示走滑断裂的构造演化与活动习性,反演断裂走滑活动历史并预测其未来行为的基础。
Early tension fracture, middle shear strike slipping or normal overturning occurred during the movement.
断裂的活动具有早期张裂、中晚期剪切走滑与正反转活动的特点。
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