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.
第二期为平行造山带的挤压缩短变形，形成区域透入性共轭破劈理或膝折带。
The second episode is characterized by NW-SE direction compression-shortening deformation with formation of two conjugate fracture cleavages or kink bands.
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