Controlled by sinistral shear stress of the regional major fault during magma emplacement, the granite distributed from the southeast to the northwest.
岩浆的侵位受区域性大断裂左旋剪切应力控制，空间上呈现由南东往北西逐渐变新的特点。
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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