This paper considers that Aerjin Mountain strike-slip fault structure is a huge tectonic zone with the property of left active anticlockwise and thrust nappes and ductile shear zone.

该文认为，阿尔金山走滑断裂构造是一巨型左行左列走滑断裂兼逆冲推覆和韧性剪切性质的断裂构造带。

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According to lots of field works, two phases of sinistral strike-slip ductile shear belts were found in the Tan-Lu fault zone.

大量的野外工作发现，郯庐断裂带存在早、晚两期韧性剪切带。

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