辽宁地区地壳垂直形变特征与地震危险性分析

孙启凯, 池国民, 畅柳, 苏广利, 田晓

孙启凯, 池国民, 畅柳, 苏广利, 田晓. 2017: 辽宁地区地壳垂直形变特征与地震危险性分析. 地震学报, 39(6): 891-898. DOI: 10.11939/jass.2017.06.007
引用本文: 孙启凯, 池国民, 畅柳, 苏广利, 田晓. 2017: 辽宁地区地壳垂直形变特征与地震危险性分析. 地震学报, 39(6): 891-898. DOI: 10.11939/jass.2017.06.007
Sun Qikai, Chi Guomin, Chang Liu, Su Guangli, Tian Xiao. 2017: Characteristics of crust vertical deformation and seismic risk analysis in Liaoning area. Acta Seismologica Sinica, 39(6): 891-898. DOI: 10.11939/jass.2017.06.007
Citation: Sun Qikai, Chi Guomin, Chang Liu, Su Guangli, Tian Xiao. 2017: Characteristics of crust vertical deformation and seismic risk analysis in Liaoning area. Acta Seismologica Sinica, 39(6): 891-898. DOI: 10.11939/jass.2017.06.007

辽宁地区地壳垂直形变特征与地震危险性分析

基金项目: 

中国地震局地震监测、预测、科研三结合课题 CEA-JC/3JH-163702

地震行业专项 201508009

中国地震局地震监测、预测、科研三结合课题(CEA-JC/3JH-163702),科技部基础性工作专项(2015FY210400)和地震行业专项(201508009)共同资助

科技部基础性工作专项 2015FY210400

详细信息
    作者简介:

    孙启凯  中国地震局第一监测中心工程师. 2010年山东农业大学测绘工程专业毕业,获工学学士学位;2013年中国矿业大学(北京)大地测量学与测量工程专业毕业,获工学硕士学位.主要从事区域精密水准监测、数据处理与分析及地震预报等工作

    通讯作者:

    孙启凯, e-mail: sqkai2006@163.com

  • 中图分类号: P315.72+5

Characteristics of crust vertical deformation and seismic risk analysis in Liaoning area

  • 摘要: 利用辽宁地区三期复测水准资料,计算得出1988—1998年和1998—2016年两个时段的地壳垂直形变速率, 并绘制相应的地壳垂直形变速率矢量图和等值线图.结合辽宁地区的区域地质背景及构造断裂活动性,分析了区域地壳垂直形变特征与地震活动性之间的相关性,明确了该区域的整体地壳垂直形变趋势及需重点关注的区域.结果表明:海城MS7.3地震后较长时间内,辽宁地区整体以继承性运动为主,辽东隆起和辽西隆起以上升为主,下辽河断陷带下沉;1998年后,辽宁地区整体形变差异量减小,该地区垂直形变正趋于稳态,垂直形变速率梯度高值区仍集中于下辽河断陷带与辽东隆起、辽西隆起的交界地带,因此该区域的潜在危险性较高,需要持续并重点关注.
    Abstract: Based on the three-issue repeated measurement data of the Liaoning area, we calculate the vertical strain rate during 1988-1998 and 1998-2016, and draw the corresponding vector graph and isoline map of the vertical deformation rate. The correlation between vertical deformation characteristics and seismic activities is analyzed combining the geological background and tectonic activity in Liaoning area, thus to identify the overall trend of deformation and to require critical attention to the areas. The results showed that Liaoning region represents as inheritance movement, Liaodong and Liaoxi uplifts exhibit an upward trend, Liaohe down-faulted zone showed subsidence for a long time after MS7.3 Haicheng earthquake; the overall amount of difference of deformation in Liao-ning area decreased since 1998, the region's vertical deformation tends to be stable. The high gradient zone of deformation rate is still concentrated in the border of Liaohe down-faulted zone, Liaodong and Liaoxi area, and then these areas exist high potential risk and need sustained and focused attention.
  • 图  1   辽宁地区区域精密水准测点、水准剖面及断裂分布

    Figure  1.   Distribution of regional precision leveling points, leveling profiles and faults in Liaoning area

    图  2   1988—1998年辽宁地区地壳垂直形变速率矢量图(a)与等值线(b)图

    Figure  2.   Vector graph (a) and isoline map (b) of vertical deformation in Liaoning area from 1988 to 1998

    图  3   1998—2016年辽宁地区地壳垂直形变矢量图(a)及等值线图(b)

    Figure  3.   Vector graph (a) and isoline map (b) of vertical deformation in Liaoning area from 1998 to 2016

    图  4   朝阳—清河门—石山水准剖面地壳垂直形变速率变化图

    Figure  4.   Vertical deformation rate of Chaoyang-Qinghemen-Shishan leveling profile

    图  5   盘山—海城—岫岩—大孤山水准剖面地壳垂直形变速率变化图

    Figure  5.   Vertical deformation rate of Panshan-Haicheng-Xiuyan-Dagushan leveling profile

    图  6   辽宁地区1988—1998年(a)和1998—2016年(b)垂直形变速率梯度图

    Figure  6.   Vertical strain rate gradient of Liaoning region in 1988-1998 (a) and 1998-2016 (b)

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出版历程
  • 收稿日期:  2017-02-05
  • 修回日期:  2017-05-24
  • 发布日期:  2017-10-31

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