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。
During early Mesozoic—Cenozoic cycle, south Tibetan—Indo protocontinent was disintegrated from the Gondwana, drifting toward the equator from southern hemisphere;
新生代板块构造旋回早期藏南—印度古陆从冈瓦纳大陆裂解出来，从南半球向赤道漂移；
应用推荐