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地震 ›› 2011, Vol. 31 ›› Issue (2): 42-49.

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利用水位资料反演华北地区构造应力场变化

孙小龙1, 刘耀炜1, 晏锐2   

  1. 1.中国地震局地壳应力研究所, 北京 100085;
    2.中国地震台网中心, 北京 100045
  • 收稿日期:2010-09-21 修回日期:2010-12-20 出版日期:2011-04-30 发布日期:2021-09-09
  • 作者简介:孙小龙(1981-), 男, 甘肃临洮人, 助研, 主要从事地震地下流体研究及地震预报。
  • 基金资助:
    中央级公益性科研院所基本科研业务专项资金(ZDJ2010-26)

Inversion of Tectonic Stress Field in the North China Region Based on Groundwater Level Data

SUN Xiao-long1, LIU Yao-wei1, YAN Rui2   

  1. 1. The Institute of Crustal Dynamics, BeiJing 100085, China;
    2. China Earthquake Networks Center, BeiJing 100045, China
  • Received:2010-09-21 Revised:2010-12-20 Online:2011-04-30 Published:2021-09-09

摘要: 本文选取华北地区观测条件较好的63口水位观测井资料, 运用小波分析法去除各井水位资料中的短期高频信息, 提取出能反映水位多年动态变化的趋势信息, 并利用各井水位趋势变化数据反演出华北地区多年构造应力场变化图像, 结合其它水文资料, 探讨了华北地区近年来的构造应力场变化特征。

关键词: 水位, 构造应力场, 华北地区

Abstract: In this paper, we selected 63 wells in north China region, which have better observing conditions. Using wavelet analysis method to remove the short-term low-frequency information in the water level data, we extracted the tendency signals which can reflect the dynamic changes of groundwater level. Change patterns of tectonic stress field in the north China region was inversed by using groundwater level data, and the tectonic stress field variation of North China region in recent years was discussed in respect to other hydrology data.

Key words: Water level, North China region, Trend changes, Tectonic stress field

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