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The evolution of the coral reefs in the middle and north parts of the South China Sea and its relation with tectonic and eustatic movements
作者姓名:Geng Xiushan  Fu Mingzuo  Wu Baoling
作者单位:First Institute of Oceanography, State Oceanic Administration, Qingdao, China;First Institute of Oceanography, State Oceanic Administration, Qingdao, China;First Institute of Oceanography, State Oceanic Administration, Qingdao, China
摘    要:In this paper, the morphogenesis, stratigraphic sequences and dates of the coral reefs in the middle and north parts of the South China Sea are discussed, the position of the distributary regions of Cenozoic coral reefs in plate tectonics, the relationships of coral-reef evolutionary characteristics and dates with sea-basin spreading. Neogene sea-water transgression and Quaternary global climate-eustatic fluctuation are expounded and proved, and the latitudinal variation of the distribution of coral reefs in various geologic times are summed up.

收稿时间:1988/10/24 0:00:00
修稿时间:1989/6/24 0:00:00

The evolution of the coral reefs in the middle and north parts of the South China Sea and its relation with tectonic and eustatic movements
Geng Xiushan,Fu Mingzuo,Wu Baoling.The evolution of the coral reefs in the middle and north parts of the South China Sea and its relation with tectonic and eustatic movements[J].Acta Oceanologica Sinica,1990,9(2):283-292.
Authors:Geng Xiushan  Fu Mingzuo and Wu Baoling
Institution:First Institute of Oceanography, State Oceanic Administration, Qingdao, China
Abstract:In this paper,the morphogenesis,stratigraphic sequences and dates of the coral reefs in the middle and north parts of the South China Sea are discussed,the position of the distributary regions of Cenozoic coral reefs in plate tectonics,the relationships of coral-reef evolutionary characteristics and dates with sea-basin spreading.Neogene sea-water transgression and Quaternary global climate-eustatic fluctuation are expounded and proved,and the latitudinal variation of the distribution of coral reefs in various geologic times are summed up.
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