Late Cenozoic tectonic movement 晚新生代构造
late cenozoic tectonic regime 晚新生代构造体制
Late Cenozoic tectonic deformation 晚新生代构造变形
LATE CENOZOIC TECTONIC DEFORMATION HISTORY 中国东西部地貌边界带晚新生代构造变形历史与青藏高原东缘隆升过程初步研究
The tectonic nature of different regions in China in the Early and Late Paleozoic, Mesozoic and Cenozoic coal-forming periods is different.
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。
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.
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。
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