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《PROGRESS IN GEOPHYSICS》 1996-01
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THE VELOCITY STRUCTURE AND THE FOCAL STRUCTURE OF THE LITHOSPHERE ONSHANTOU-LUZONISLAND

Chen Xuebo; Li Jinsen; Wang Enfu; Si Hongbo (Institute of Crustal Dynamics S.S.B. Beijing 100085)  
Shantou-Luzon island has been devided into the Palaeozoicera crust of Huanan continental margin,the late Palaeozoic-Mesozoic crust of the shelf region, the Mesozoic era-the early Tertiary period transition crust of the continental slope zone, the Cenozoic sea basin oceanic crust of the Nanhai sea, the Mesozoic-Cenozoic island are crust of the Luzon island and the oceanic crust of the east Luzon trough and other crustal structure, and the boundary fault structure among the above mentioned crustal structure and feature has been defined by the velocity structure sections of the lithosphere from Shantou to Luzon. The mechanics feature of focus and controling and generating earthquake structure are established preliminery combined with focus distribution and focus mechanism on the both sides of the south and north Huanan shelf basin mountain range structure zone; It is suggested that Taiwan shoal Ms7.3 earthquake on September 16, 1994 is a crust-mantle earthquake of the plate margin, and then it is sensed over 1000km. The reason for displaying normal fault fearure of Manila trench subduction zone to be considered is a submarine graben structure of Malila trench and mantle rise of sea basin lithosphere of Nanhai sea. which is passive or transform subduction zone; The east Luzon trough belongs to subduction zone of Philippine Sea; The quasi-three layers distribution of lithosphere slab focal depth on both sides of the east and the west of Luzon island subduction zone may show the relevant low velocity phorogenesis layer existed in the lithosphere slab of the subduction zone.
【CateGory Index】: P315.33
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