SEISMOLOGY AND GEOLOGY ›› 2009, Vol. 31 ›› Issue (2): 233-246.DOI: 10.3969/j.issn.0253-4967.2009.02.004

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HE Zhong-tai, MA Bao-qi, LU Hai-feng, WANG Jin-yan   

  1. Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China
  • Received:2008-04-24 Revised:2008-07-20 Online:2009-03-11 Published:2009-11-27


何仲太, 马保起, 卢海峰, 王金艳   

  1. 中国地震局地壳应力研究所, 北京, 100085
  • 作者简介:何仲太,男,1982年生,2004年毕业于吉林大学,2007年在中国地震局地壳应力研究所获硕士学位,主要从事地震地质与工程地震研究,电话:010-62842649,
  • 基金资助:

Abstract: Lots of different ideas stay on whether the Dongbeiwang-Xiaotangshan Fault in the northwest of Beijing exists or how it displays and acts.This paper analyzes the present seismic prospecting data and drill logs from exploration of active faults in Beijing urban areas,and reaches conclusion that the Dongbeiwang-Xiaotangshan Fault does exist as a subsurface fault and it is 40km long,trending NNE.Divided by the Nankou-Sunhe Fault,we name its northeast segment as the Xiaotangshan Fault and the southwest segment as the Dongbeiwang Fault.The Xiaotangshan Fault is active in early Pleistocene but not in middle Pleistocene.The Dongbeiwang Fault is active in the end of mid-Pleistocene but not in late Pleistocene.

Key words: Dongbeiwang-Xiaotangshan Fault, seismic prospecting, drill logs, buried fault, Beijing

摘要: 对位于北京市西北侧的东北旺-小汤山断裂是否存在、走向与活动性的认识长期以来一直存在较大差异。通过新近开展的北京城市活断层探测工作中的物探数据与钻孔联合剖面分析,认为东北旺-小汤山断裂是存在的,为一条隐伏断裂,长约40km,走向NNE,倾向SE。以南口-孙河断裂为界,该断裂东北段称之为小汤山断裂,西南段称之为东北旺断裂。小汤山断裂的最新活动时代为早更新世或中更新世早期,中更新世中期以来不活动。东北旺断裂的最新活动时代为中更新世末期,晚更新世以来不活动。

关键词: 东北旺-小汤山断裂, 地震勘探, 钻孔联合剖面, 隐伏断裂, 北京

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