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。
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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