摘要
Multiperiod important tectonic boundaries develops in Guizhou,Wuling orogeny is the embodiment of shrinkage and extinction of Nanhua narrow oceanic basin,the ocean-continent transition of South China block by convergence and collision by Yangtze oldland and Cathaysian oldland,Wuling sub-orogenic belt of Jiangnan compound orogenic belt formed.Guangxi movement is the embodiment of shrinkage and extinction of Nanhua valley,the ocean-continent transition of South China block by re-convergence and re-collision by Yangtze oldland and Cathaysian oldland,Caledonian sub-orogenic belt of Jiangnan compound orogenic belt formed.Yanshan movement made Guizhou affected from east and west direction the same time,put Guizhou the margin of its orogenic belt,the orogenic center of the east plate maybe near Beihai-Pingxiang-Shaoxing zone,is the embodiment of orogeny in South block,Yanshan sub-orogenic belt of Jiangna orogenic belt formed,the west orogenic center maybe Ailao mountain.Himalaya Neotectonism made Guizhou experiences low-lying East West early,stable and flat in middle period and low-lying West East now in platform.