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《地球科学》 1991-05
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ON KINEMATICS OF LATE PROTEROZOIC-TRIASSIC PALEOPLATES IN EASTERN CHINA

Zhu Hong Wan Tianfeng (China University of Geosciences, Beijing 100083)  
Depending on the more reliable existing paleomagnetism data selected seriously, comprehending the rock deformation, sedimentary paleogeography, magmatism and metamorphism data, the Late Proterozoic-Triassic paleotectonic sketches of the plates in eastern China have been drawn. Since the Jinning event,up to the entire period of Paleozoic, the extension has existed in the China-Korea plate and the plates of South China, which maintained the considerable distance, migrated continuously in the low and intermediate latitude zone,and thus made different tectonic evolutions. Since the Triassic, they have come to amalgamate gradually. In the end of Early Triassic, the Lincang-Baoshan terrane amalgamated to the western Yangtze plate, the Xianggui plate probably inserted into the South China plate. In the late stage of Middle Triassic ,the South China plate collided with Yangtze plate and the widespread folding was developed in them. Up to the end of the Late Triassic, the Yangtze plate then collided with the China-Korea plate, the plates of eastern China amalgamated, the tectonic framework of which was fundamentally set up.
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