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东海陆架盆地西缘南北向深大断裂
引用本文:刘英会,黎津,余学中.东海陆架盆地西缘南北向深大断裂[J].物探与化探,2007,31(6):518-519,525.
作者姓名:刘英会  黎津  余学中
作者单位:中国国土资源航空物探遥感中心,北京,100083
摘    要:通过对航磁资料的深入研究,首次在东海陆架盆地西缘圈定出1条南北向深大断裂,为陆架盆地控盆深大断裂;推断了该断裂的形成时期,并就这条断裂对火成岩及构造走向的控制作用、地质意义进行了分析.

关 键 词:航磁  东海陆架盆地  西缘深大断裂
文章编号:1000-8918(2007)06-0518-02
收稿时间:2007-09-01
修稿时间:2007年9月1日

THE NE-TRENDING DEEP FAULT ON THE WESTERN EDGE OF CONTINENTAL SHELF BASINS OF THE EAST CHINA SEA
LIU Ying-hui,LI Jin,YU Xue-zhong.THE NE-TRENDING DEEP FAULT ON THE WESTERN EDGE OF CONTINENTAL SHELF BASINS OF THE EAST CHINA SEA[J].Geophysical and Geochemical Exploration,2007,31(6):518-519,525.
Authors:LIU Ying-hui  LI Jin  YU Xue-zhong
Institution:China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China
Abstract:According to a preliminary study of the aeromagnetic data,a deep NS-trending fault was recently recognized which controls the western edge of continental shelf basins of the East China Sea.The authors have studied the formation period of the NS-trending fault,and also analyzed the geological significance of this fault in controlling igneous rocks and the strike of the tectonic line.
Keywords:aeromagnetic survey  continental shelf basins of the East China Sea  deep fault on the western edge
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