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首都圈地壳网格化三维结构
引用本文:嘉世旭,齐诚,王夫运,陈棋福,张先康,陈颙.首都圈地壳网格化三维结构[J].地球物理学报,2005,48(6):1316-1324.
作者姓名:嘉世旭  齐诚  王夫运  陈棋福  张先康  陈颙
作者单位:中国地震局地球物理勘探中心,郑州,450002;中国科学院地质与地球物理研究所,北京,100029;中国地震局分析预报中心,北京,100036
基金项目:国家自然科学基金重点项目(40234038),基础研究重大项目前期研究专项(2001CCA02100),地震科学联合基金(105078,101026)资助
摘    要:通过对首都圈地区不同时期的18条深地震测深(DSS)测线资料的重新统一处理,形成采样网格密度为025°×025°×(2~5)km的速度网格化数字地壳;通过对三维数据的可视化,得到了首都圈地壳不同走向、不同圈层的截面图像;从不同的视角、不同的方面探讨了控制首都圈地壳的北部燕山隆起、西南部太行隆起和东南部裂陷盆地等三大地质单元的构造特征以及接触带张家口-渤海断陷带的构造性质,进一步研究首都圈地壳内部结构构造与灾害性地震的孕发机制的关系.

关 键 词:首都圈  深地震测深  地壳三维结构
文章编号:0001-5733(2005)06-1316-09
收稿时间:2004-01-05
修稿时间:2004-01-052006-03-09

Three-dimensional crustal gridded structure of the Capital area
JIA Shi-Xu,QI Cheng,WANG Fu-Yun,CHEN Qi-Fu,ZHANG Xian-Kang,CHEN Yong.Three-dimensional crustal gridded structure of the Capital area[J].Chinese Journal of Geophysics,2005,48(6):1316-1324.
Authors:JIA Shi-Xu  QI Cheng  WANG Fu-Yun  CHEN Qi-Fu  ZHANG Xian-Kang  CHEN Yong
Affiliation:1.Research Center of Exploration Geophysics, China Earthquake Administration, Zhengzhou 450002, China 2 Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China 3 Center for Analysis and Prediction, China Earthquake Admini
Abstract:After unified reprocessing of the 18 DSS profile data that are got in various periods in the Capital area, a digital crust model of velocity grid is obtained with sampling density 025°×025°×(2~5)km. Through 3 D data visualization, images of slice sections in different strikes and at depths are produced. Based on these images, the tectonic characteristics of the three main geological units, which control the crust in the Capital area including the Yanshan uplift in north, the Taihang uplift in southwest and the rift depression basin in southeast, and the tectonic features of the contact zone——the Zhangjiakou Bohai Sea seismic zone are studied from various aspects. Furthmore, the relation between the inner structure of the crust in the Capital area and the generation of catastrophic earthquakes is studied.
Keywords:Capital area  Deep seismic sounding  3-D crustal structure
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