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地震 ›› 2021, Vol. 41 ›› Issue (1): 180-190.doi: 10.12196/j.issn.1000-3274.2021.01.014

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辽宁地区时变重力场源变化特征分析

贾晓东1, 翟丽娜1, 陈石2,3   

  1. 1.辽宁省地震局, 辽宁 沈阳 100034;
    2.中国地震局地球物理研究所, 北京 100081;
    3.北京白家疃国家地球科学野外观测研究站, 北京 100095
  • 收稿日期:2020-09-07 修回日期:2020-11-11 出版日期:2021-01-31 发布日期:2021-01-28
  • 通讯作者: 陈石,研究员。E-mail:chenshi@cea-igp.ac.cn
  • 作者简介:贾晓东(1980-),男,山东兖州人,高级工程师,主要从事地壳形变与地球动力学分析研究。
  • 基金资助:
    震情跟踪青年项目(2021010204); 星火计划青年项目(XH21013Y); 地震预测预警运维项目(2240505); 星火计划攻关项目(XH19059)

Analysis on the Characteristics of Time-varying Gravity Field Source Changes in Liaoning Area

JIA Xiao-dong1, ZHAI Li-na1, CHEN Shi2,3   

  1. 1. Liaoning Earthquake Agency, Shenyang 110034, China;
    2. Institute of Geophysics, China Earthquake Administration, Beijing 100081, China;
    3. Beijing Baijiatuan Earth Science National Observation and Research Station, Beijing 100095, China
  • Received:2020-09-07 Revised:2020-11-11 Online:2021-01-31 Published:2021-01-28

摘要: 地震重力分析通过研究时变重力场变化获取地球内部介质物性变化信息。 采用贝叶斯重力网平差方法对辽宁地区2011—2014年共计四年7期的流动重力观测资料进行处理, 对研究区重力观测网总体监测能力做出分析, 选用欧拉反褶积对研究区的重力变化场源深度及空间分布特征进行反演和解释。 通过反演计算发现, 在2013年灯塔MS5.1地震前沈阳—辽阳地区重力变化较大, 形成高梯度带, 反映该地区地震活动性增强; 而欧拉反褶积计算反演地下介质场源深度在10~40 km, 与地震实际发生深度相符, 且集中在断裂带附近。 本研究可为研究辽宁地区深部孕震环境特征提供一定参考。

关键词: 时变重力场, 贝叶斯重力网平差, 流动重力, 欧拉反褶积, 密度变化

Abstract: Seismic gravity analysis can be used to obtain the physical properties of the earth by studying the change of the time-varying gravity. In this paper, the Bayesian gravity network adjustment method is used to process the mobile gravity observation data for a total of 7 periods of four years in Liaoning from 2011 to 2014, evaluate and analyze the overall monitoring capability of the gravity observation network in the study area,and employ the Euler deconvolution method to inverse field source parameters,before the lighthouse MS5.1 earthquake occurred in 2013. The results show that the gravity in the Shenyang-Liaoyang area changed greatly, forming a high-gradient zone, reflecting the increase in seismic activity in this area; while the depth of the underground medium field source inverted by Euler deconvolution is 10~40 km, It is consistent with the actual depth of the earthquake and is concentrated near the fault zone. The research results can further provide a certain reference for studying the characteristics of the deep seismogenic environment in Liaoning.

Key words: Time-varying gravity field, Bayesian gravity network adjustment, Campaign gravity survey, Euler deconvolution, Density variation

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