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《GEOSCIENCE》 1999-01
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RESEARCH ON THE INTRAPLATE DEFORMATION VELOCITY OF CHINA IN MESO CENOZOIC

Wan Tianfeng Ren Zhihe(China University of Geosciences, Beijing, 100083)  
Depending on 11803 chemical total analysis data of common elements for magmatic rocks of Meso Cenozoic, using the Sugisaki′s method to determine the intraplate deformation velocity from the chemical composition of rocks, the intraplate shortening(closing), and extension velocities of different tectonic stages for China were obtained. The intraplate average shortening velocities are 5 4~5 6cm/a in the Indosinian, Yanshanian and Sichuanian stages, 4 5cm/a in the North Sinian stage., 5 2cm/a at the western China in the Himalayan stage, and 2 5~2 8cm/a in the Neotectonic stage. From the Triassic to Oligocene, there was still the Tethys Ocean with lower extension velocity(0 2~1 6cm/a)in the southwestern area of China. Since the Himalayan stage, the collision further developed in the southwestern China, the Qinghai Xizang Plateau was uplift and the crust was shortening; however, the weak extensions(0 1~0 6cm/a)showed commonly in the eastern China.
【Fund】: 国家计委国土司资助 国土资源部科技司资助
【CateGory Index】: P534.62,P542.4
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