纵弯叠加褶皱地区岩石有限应变特征是所受历次变形的综合结果。
The features of rock finite strain in the superimposed fold area under buckling are comprehensive results of multiphase deformation.
叠加褶皱与拼接带具有成生联系，且各自代表了不同构造部位的变形特点。
Therefore, the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in di.
叠加褶皱与拼接带具有成生联系，且各自代表了不同构造部位的变形特点。
Therefore, the superimposed fold system and the suture zone are interrelated in origin and they have the distinct deformation features in different structural positions.
除具陆相盆地的一般特征外，还具有十分突出的叠加褶皱变形特征，因而极为少见。
It has not only common characters of continental basins, but also remarkable superimposed fold deformation.
因此，正确地识别叠加褶皱，就成为查明变质岩区构造及变形历史的关键之一，也是建立变质岩层层序最需重视的问题。
So to recognize superposed folds correctly is one of the keys to identify the structures and deformation history in metamorphic terrains.
西部变形弱、以近ew向宽缓褶皱变形为主，东部变形强、并叠加了NE向褶皱和逆冲断层变形。
In the Western part the deformation was weak only EW-trending open folds occurred while in the Eastern part deformation was stronger but some NE folds and thrusts superposed on the EW folds.
西部变形弱、以近ew向宽缓褶皱变形为主，东部变形强、并叠加了NE向褶皱和逆冲断层变形。
In the Western part the deformation was weak only EW-trending open folds occurred while in the Eastern part deformation was stronger but some NE folds and thrusts superposed on the EW folds.
应用推荐