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.
中国早、晚古生代、中生代和新生代成煤期的大地构造性质，在各个地区可有不同。
The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.
本文对晚新生代贵州喀斯特地貌演进的三大控制因素 ，即地质基础、新构造运动及挽近气候波动进行了分析论证。
In this paper, three determined factors influencing on the evolution of karst geomorphology of upper Cenozoic in Guizhou, e.
通过对东大滩—东温泉地区的路线地质观测与构造填图，在东昆仑南部发现晚新生代大型逆冲推覆构造系统。
A large-scale Late Cenozoic overthrust system has been found in the southern East Kunlun Mountains through tectonic mapping and geological reconnaissance in the Dongdatan-East Wenquan area.
矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。
The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
矿山梁构造几何学上表现为一个双重构造：浅层是一个晚三叠世形成的断层转折褶皱；深层则是在新生代形成的三个逆冲岩片叠置所构成的隐伏堆垛背斜构造。
The key structure in this area is a duplex that comprises of a shallow fault-bend fold of the Late Triassic and a deep blind stacking anticline imbricated by three thrust sheets of Cenozoic age.
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