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东海陆架及邻区新构造运动特征
引用本文:李达,张维冈,李晶.东海陆架及邻区新构造运动特征[J].海洋地质动态,2010,26(1).
作者姓名:李达  张维冈  李晶
作者单位:中国海洋大学海洋地球科学学院,青岛,266100;海底科学与探测技术教育部重点实验室,青岛,266100
摘    要:东海位于大陆板块与大洋板块接合部位,受两大板块活动的影响,新构造期海域活动强烈。我们结合最新收集资料文献,从地形地貌、地热异常、断块体的水平位移和垂直差异升降、活动断裂、地震活动及岩浆岩活动等方面,着重论述了东海陆架及邻区的新构造运动特征。为东海海域新构造分区、地震预测、区域稳定性评价等提供若干资料及依据。

关 键 词:陆架区  新构造运动  东海  

NEOTECTONIC CHARACTERISTICS OF EAST CHINA SEA CONTINENTAL SHELF AND ADJACENT REGIONS
LI Da,ZHANG Wei-gang,LI Jing.NEOTECTONIC CHARACTERISTICS OF EAST CHINA SEA CONTINENTAL SHELF AND ADJACENT REGIONS[J].Marine Geology Development,2010,26(1).
Authors:LI Da  ZHANG Wei-gang  LI Jing
Institution:1 College of Marine Geosciences;Ocean University of China;Qingdao 266100;China;2 MOE Key Laboratory of Seafloor Sciences and Detection Techniques;China
Abstract:The East China Sea,located at the juncture of a continental plate and an oceanic plate and influenced under motions of these two great plates,had intensive marine neotectonic activities.The authors put emphasis on neotectonic characteristics of East China Sea continental shelf and adjacent regions by using the latest data in the aspects of topographic and geomorphic features,geothermal anomalies,horizontal displacement and vertical differential movements of fault blocks,active faulting,earthquake activities...
Keywords:continental shelf region  neotectonic movement  the East China Sea  
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