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《Progress In Geophysics》 2002-01
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Preliminary Study on Post-Late Paleozoic Kinematics of the Main Blocks of the Paleo-Asian Ocean

REN Shou-mai 1 HUANG Bao-chun 2 (1.College of Earth Sciences, Jilin University, Changchun, 130061,China; 2.Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100101,China)  
On the basis of the geological and paleomagnetical results from some blocks of the Paleo-Asian Ocean, we preliminary summarized the location and time of the suturing between the North China block and Siberia and expatiated the tectonic evolution history of Hinggan-Mongolian orogen since the late Paleozoic. However, these two blocks showed a different amount of southward movement, which may be caused by the stress eliminating of the orogen. Kinematics sketch between North China block and Siberia were also discussed. During the early Jurassic, northward drift of Siberia reached a climax and then turned to southward movement. As a result, the North China block may show significant southward movement during that time. Since the early Jurassic, the subduction of Kula plate may cause the North China block turn to northward movement with counterclockwise rotation of 10°. We inferred that it is this northward movement and counterclockwise rotation caused the formation of the arc-structure fold belt in Northeast China.
【Fund】: 中国科学院知识创新工程项目 (KZCX2~ 10 4)
【CateGory Index】: P541
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