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《Donghai Marine Science》 2004-03
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The crustal structure character of East China Sea

FANG Yin-xia,LIU Jian-hua (Second Institute of Oceanography, SOA, Laboratory of Submarine Geosciences, SOA,Hangzhou 310012, China)  
This paper presents actuality of investigation and study of the crustal structure characters of East China Sea at home and abroad. Based on the lots of investigation and study achievements and the difference of the crustal velocity structure from west to east, East China Sea is divided into three parts such as East China Sea shelf zone, Okinawa Trough zone and the Ryukyu arc-trench zone. East China Sea shelf zone mostly has three velocity layers, such as the sediment blanket layer (the velocity is 5.8~5.9 km/s), the basal layer(the velocity is 6.0~6.3 km/s),and the lower crustal layer(the velocity is 6.8~7.6 km/s).So this zone belongs to the typical continental crust. The Okinawa Trough zone is located in the transitional belt between the continental crust and the oceanic crust. It still has the structure characters of the continental crust, and no any formation of the oceanic crust, but its crust of the central trough has thined. The Ryukyu arc-trench zone is belonging to the transition type crust as a whole, but the side of the trench is already belonging to the oceanic crust. And the northwest Philippines Basin to the east of the Ryukyu trench absolutely belongs to the typical oceanic crust.
【Fund】: 国家重点基础研究发展规划资助项目(G20000467)
【CateGory Index】: P736.14
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