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SOUTH CHINA DEFINED AS PART OF TETHYAN ARCHIPELAGIC OCEAN SYSTEM

Yin Hongfu Wu Shunbao Du Yuansheng Peng Yuanqiao (Faculty of Earth Sciences, China University of Geosciences, Wuhan430074)  
When the rifted blocks of Gondwana and Eurasian supercontinents were drifting, the ocean basin in front of the drifting blocks may have subducted and disappeared, but a new ocean may have developed from a rift valley behind the drifting blocks, as suggested in the Tethyan archipelagic ocean model. The ocean basins that occurred in sequence may have been classified as different stages of the Paleo_, Meso_ and Neo_Tethys. The multi_phase process from the riftogenesis, block drift to subduction may have distinguished the Tethys from such “clean” oceans as the Atlantic Ocean and the Pacific Ocean. In different evolutionary stages of the Tethys, the Tethys has always remained an archipelagic ocean, a mosaic of seas and lands in various degrees of dispersion and integration, for examples, the rifted blocks, rifts and seaways; micro_plates and micro_oceans; island arcs and marginal seas. South China, part of the archipelagic ocean system of Tethys, is composed of the Qinling micro_plate, the Yangtze plate (including the Lower Yangtze block, the Qamdo_Simao block, the Yidun block and the Songpan_Garze block), the Cathaysian plate, the Sibumasu plate (Baoshan) and the Indo_China_South China Sea plate. The South China has been separated from the North China plate and also split into different smaller plates by the Shangxian_Danfeng micro_ocean, the Mianxian_Lueyang micro_ocean, the South China micro_ocean and the Paleo_Tethys ocean. This paper presents the relationship between Yangtze and Cathaysia, the relationship among Qinling, Yangtze and North China, and examines the rifted blocks along the western side of the Yangtze plate, as well as the pro_Gondwana rifted blocks. The paleo_oceanic maps are reconstructed from tectonic, sedimentary, paleontologic and paleomagnetic data. Plate tectonics of the archipelagic ocean system is characterized by soft collison, polycyclicity and orogenic longevity. Its plate collision resulted from multi_phase micro_collision of island or block accretion. The velocity of each micro_collision is a difference between, rather than a sum of, the velocity of two colliding blocks. The total mass of the two colliding blocks is so small that no orogeny may have occurred. This is what we called the “soft collision”. Polycyclicity follows the concept by Huang Jiqing. Each micro_collision is usually ensued by a relaxed or extensional phase. In this sense, the orogeny did not always immediately follow each collision. Sometimes, the orogeny may have been deferred until after 100Ma or longer years, resulting in the longevity of an orogeny.
【Fund】: 国家自然科学基金
【CateGory Index】: P736.222,P531
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