... new tectonic movement 新构造运动 Late Cenozoic tectonic movement 晚新生代构造 cyclicity of tectonic movement 构造运动的旋回性 ...
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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.
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