准噶尔盆地南缘的晚新生代构造变形被认为是天山地区对印度和欧亚板块的碰撞与会聚作用过程的构造响应。
The late Cenozoic deformation is considered as a response to the India and Eurasia plate collision and continuous compression.
重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。
This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.
论述了祁连山构造带新生代以来的变形过程及形成机制。
In this paper, the deformation process and deformation mechanism of Qilianshan Structure Belt, since Cenozoic era, have been discussed.
川西北盆地在新生代是一个典型的构造叠加区域，来自龙门山和米仓山的变形在此相互作用。
The Northwest Sichuan Basin is a typical tectonic superposition region in Cenozoic, where the deformations transferred from the Longmenshan and Micangshan affected together.
青藏高原新生代伸展地堑构造是高原经历早期地壳强烈缩短变形之后，在深部动力学机制作用下快速隆升的产物。
The Cenozoic extensional grabens on the Qinghai-Tibet plateau are the product of rapid uplift of the plateau caused by the deep dynamic mechanism after earlier strong crustal shortening.
从构造样式、沉积特征、断层组合等方面探讨了黄骅盆地海岸线两侧右旋走滑构造变形的存在，指出结晶基底的不均匀性是NNE向基底隐伏走滑带形成和新生代盖层走滑构造产生的控制因素。
The unevenness of crystalline basement is found to be the governing factor for forming the NNE-striking blind basement strike-slip zone and the strike-slip tectonics in the Cenozoic platform cover.
第四期变形为新生代晚期东西向伸展机制下产生的南北向地堑构造。
The fourth phase is that the NS graben structure was produced by EW expanding mechanism in late Cenozoic.
新生代构造冲断位移量以及造成早期构造抬升由北向南逐渐减小，反映新生代变形强度由北向南的减弱。
The Cenozoic deformation intensity becomes much weaker from the north to south and results in the smaller displacement and structural uplift of the thrust folds.
区内新构造运动迹象明显，在地貌、新生代地层变形、断裂新活动等方面均有反映。
The sign of neotectonism in this area is obvious, which is reflected in land form, formation deformation in new born zone, new movement of fault, etc.
区内新构造运动迹象明显，在地貌、新生代地层变形、断裂新活动等方面均有反映。
The sign of neotectonism in this area is obvious, which is reflected in land form, formation deformation in new born zone, new movement of fault, etc.
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