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。
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.
大量透入性变形和巨型大陆造山带内部构造显示非刚性特征。
The pervasive deformation and internal structure of wide continental orogenic belts indicate non-rigid behavior.
文中重点介绍了乌拉尔—阿曼巨型线性构造带和阿尔卑斯大陆碰撞带的影像特征和地质意义。
In this paper, we put emphasis on the introduction of the image characteristics and geological significance of Urals-Oman giant lineament and Alps continental collision.
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