新乡及邻区三维地壳速度结构
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  • 英文篇名:3-D crustal velocity structure in Xinxiang and its adjacent regions
  • 作者:莘海亮 ; 刘明军 ; 张元生 ; 戴骜鹏
  • 英文作者:XIN Hai-liang;LIU Ming-jun;ZHANG Yuan-sheng;DAI Ao-peng;Research Center of Exploration Geophysics,China Earthquake Administration;Lanzhou Institute of Seismology,China Earthquake Administration;
  • 关键词:新乡及邻区 ; 三维速度结构 ; 震源参数 ; 联合反演
  • 英文关键词:Xinxiang and its adjacent regions;;3D velocity structure;;source parameters;;combined inversion
  • 中文刊名:DQWJ
  • 英文刊名:Progress in Geophysics
  • 机构:中国地震局地球物理勘探中心;中国地震局兰州地震研究所;
  • 出版日期:2014-08-15
  • 出版单位:地球物理学进展
  • 年:2014
  • 期:v.29;No.126
  • 语种:中文;
  • 页:DQWJ201404012
  • 页数:7
  • CN:04
  • ISSN:11-2982/P
  • 分类号:103-109
摘要
应用区域地震台网1981-2011年的地震到时资料,对新乡及邻区地壳三维速度结构和震源参数进行了联合反演,获得了该区地壳的三维速度结构图像.结果显示:0~4 km深度层位的速度分布基本反映出了研究区浅部地形的分布特征,凹陷盆地速度低,山脉位于速度的过渡区,隆起区多位于高速区,横向速度分布差异较大;其余各深度层速度横向分布存在非均匀性,与地形分布特征也存在着一定的联系;速度剖面整体显示区域地壳可以分为上、中、下三个分层,上地壳速度横向变化较小;中、下地壳的界面速度横向起伏变化较大,局部地区呈现上隆或凹陷状;根据速度的分布差异,以及所勾画的深部断裂的轮廓展布,对该区的深部构造有了较深认识:汤西断裂、汤东断裂显示错断较深,倾角较陡,有延伸到中地壳底部的趋势;郑州-开封断裂带、新乡-商丘断裂,与人工地震剖面相同位置处及地质剖面有着较好的对应.
        Based on the joint inversion of 3D crustal velocity structure and focal parameters in Xinxiang and its adjacent areas when applying arriving time data in 1981-2011,we obtained three-dimensional(3D)crustal velocity structural images.Results shows that the velocity distribution in the range of 0~4 km depth describe characteristics in the shallow part—the velocity in sag basin is low;mountains are in the velocity transition region;the uplift area is mostly in highvelocity area;lateral velocity distribution vary a lot;other layers' lateral velocity distribution is heterogeneity,being related with the topographical distribution.By means of velocity profile,the crust in the study area could be divided into three layers—upper,middle and lower.For the lateral velocity change,it vary less in the upper mantle while more in the middle and lower mantle interface,rising or sagging in local areas.According to the velocity distribution difference and contour of the deep fault, we get a comprehensive understanding of this area's deep structure.There is deep leaps in Tangxi and Tangdong faults where the dip is steep,extending to the bottom of the middle crust.ZhengzhouKaifeng fault and Xinxiang—Shangqiu fault have a good corresponding with the same place on the artificial seismic profile and geological profile.
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