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现代地质 ›› 2008, Vol. 22 ›› Issue (2): 288-293.

• 遥感应用 • 上一篇    下一篇

长春市区尖山子—卡伦断层活动性研究

盛俭1,薄景山2,佴磊1,张羽3   

  1. 1吉林大学 建设工程学院,吉林 长春130026;2防灾科技学院,河北 燕郊101601;3吉林省地震局,吉林 长春130000
  • 收稿日期:2007-11-15 修回日期:2008-02-18 出版日期:2008-02-20 发布日期:2008-02-20
  • 作者简介:盛俭,男,博士研究生,1979年出生,地质工程专业,主要从事地质工程的研究工作。 Email:sj2984@sina.com
  • 基金资助:

    国家发展计划委员会“十五”重点项目(20041138147)

Activity of JianshanziKalun Fault in Changchun City

SHENG Jian1, BO Jing-shan2, NAI Lei1 , ZHANG Yu3   

  1. 1College of Construction Engineering,Jilin University,Changchun,Jilin130026,China;  2Institute of Disaster Prevention Science and
    Technology,Yanjiao,Hebei101601,China; 3Seismological Bureau of Jilin Province,Changchun,Jilin130000,China
  • Received:2007-11-15 Revised:2008-02-18 Online:2008-02-20 Published:2008-02-20

摘要:

尖山子—卡伦断层是贯穿长春市区的一条主要断裂。以往对其缺乏系统的研究,只是通过地貌和水文地质的一些资料,判断它的大致展布形态和活动时代。本次调查通过遥感、电法、探地雷达、浅层人工地震以及钻孔联合剖面相结合的方法,比较准确地确定了尖山子—卡伦断层在长春市范围内的空间位置、产状和活动时代。调查结果显示,尖山子—卡伦断层错断了白垩系地层,但没有扰动上覆的中更新统地层,以此推断长春市范围内尖山子—卡伦断层在中更新世以来是不活动的。

关键词: 尖山子—卡伦断裂, 位置, 活动性, 长春市

Abstract:

JianshanziKalun fault is an important fault which runs through the Changchun City. Former study on this fault was just based on physiognomy and hydrogeological data. The location, extending direction, orientation and activity of JianshanziKalun fault was acquired by remote sensing technique,electrical method, shallow seismic exploration, ground penetrating radar and united boring hole section. The result of investigation revealed that JianshanziKalun fault had been inactive since MiddlePleistocene epoch.

Key words: JianshanziKalun fault, location, activity, Changchun City

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