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北京市浅层剪切波速与隐伏构造关系研究
引用本文:玄月,吴涛,刘轩,李伟华,王金萍.北京市浅层剪切波速与隐伏构造关系研究[J].华北地震科学,2014,32(2):25-28.
作者姓名:玄月  吴涛  刘轩  李伟华  王金萍
作者单位:1. 中国地震应急搜救中心,北京100049;北京吉奥星地震工程勘测研究院,北京100049
2. 中国地震应急搜救中心,北京,100049
基金项目:中国地震应急搜救中心青年科技基金项目
摘    要:以北京平原区地震钻孔为基础资料,建立三维剪切波速速度模型,获得了2个代表性的波速剖面,研究其与地质构造和隐伏断裂之间的关系,结果表明:北京平原区新构造运动和隐伏断裂活动对晚第四纪地层沉积和发育具有控制作用,而且浅层剪切波速的差异性也为隐伏构造的位置确定提供了帮助。

关 键 词:剪切波速  断层  地质构造  北京平原区  第四系

Study of Relationship between Shallow Shear Wave Velocity and Buried Structure in Beijing Plain
XUAN Yue,WU Tao,LIU Xuan,LI Wei-hua,WANG Jin-ping.Study of Relationship between Shallow Shear Wave Velocity and Buried Structure in Beijing Plain[J].North China Earthquake Sciences,2014,32(2):25-28.
Authors:XUAN Yue  WU Tao  LIU Xuan  LI Wei-hua  WANG Jin-ping
Institution:XUAN Yue, WU Tao, LIU Xuan, LI Wei-hua, WANG Jin-ping (1. National Earthquake Response Support Service, Beijing 100049, China; 2. Beijing Ji'aoxing Earthquake Engineering Reconnaissance Institute, Beijing 100049, China)
Abstract:In this paper, we use drill logging to obtain a shallow 3-D shear wave velocity structure model, and select 2 typical velocity profiles to explain the relationship between the structure and buried fault. The results show that the late quaternary Sedimentary in Beijing plain are controlled by the new tectonic and buried fault movement. Moreover, the difference of shear wave velocity plays an important role in the precise positioning of the buried structure.
Keywords:shear wave velocity  fault  geological structure  Beijing plain  quaternary
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