[1]王新安,黄继攀,雍珊珊,等.2017 MS7.0九寨沟地震前后AETA数据分析[J].华南地震,2020,40(01):21-28.[doi:10.13512/j.hndz.2020.01.003]
 WANG Xinan,HUANG Jipan,YONG Shanshan,et al.Analysis of AETA Data before and after the MS 7.0 Jiuzhaigou Earthquake in 2017[J].South China journal of seismology,2020,40(01):21-28.[doi:10.13512/j.hndz.2020.01.003]
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2017 MS7.0九寨沟地震前后AETA数据分析()
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华南地震[ISSN:1006-6977/CN:61-1281/TN]

卷:
40
期数:
2020年01期
页码:
21-28
栏目:
地震科学研究
出版日期:
2020-03-31

文章信息/Info

Title:
Analysis of AETA Data before and after the MS 7.0 Jiuzhaigou Earthquake in 2017
文章编号:
1001-8662(2020)01-0021-08
作者:
王新安123黄继攀123雍珊珊12张 兴3梁意文4
1. 北京大学深圳研究生院集成微系统科学工程与应用重点实验室 广东 深圳 518055;2. 北京大学深圳地震监测预测技术研究中心,广东 深圳 518055;3. 北京大学信息科学技术学院,北京 100871;4. 武汉大学计算机技术学院,武汉 430072
Author(s):
WANG Xin’an123HUANG Jipan123YONG Shanshan12ZHANG Xing3LIANG Yiwen4
1. The Key Laboratory of Integrated Micro-systems Science and Engineering Applications,Peking University Shenzhen Graduate School,Shenzhen 518055,China;2. Earthquake Monitoring and Prediction Technology Research Center,Peking University Shenzhen Graduate School,Shenzhen 518055,China;3. School of electronics engineering and computer science,Peking University,Beijing 100871,China;4. Computer School of Wuhan university,Wuhan 430072,China
关键词:
九寨沟地震AETA地声电磁扰动
Keywords:
Jiuzhaigou earthquakeAETA Geo-soundElectromagnetic disturbance
分类号:
P315.62
DOI:
10.13512/j.hndz.2020.01.003
文献标志码:
A
摘要:
九寨沟地震发生时,中国四川省内布设了 36个AETA台站,形成了小区域的监测台阵。通过研究了这些台站的震前数据,发现13个台站的数据出现了异常。其中10个台站出现地声异常,6个台站出现电磁扰动异常。同时,一种与日升日落几乎同步的电磁扰动波形-SRSS波被发现,该波形在震中周边多处出现。这些异常很可能是九寨沟地震的前兆异常。AETA台阵成功实现了单一震例下多分量多台站前兆异常的捕捉。未来拟进一步加密AETA台阵来实现更深入的研究。
Abstract:
When the Jiuzhaigou earthquake occurred,36 AETA stations were set up in Sichuan Province, forming a small regional monitoring array. In this paper,the pre earthquake data of these stations are studied, and the data of the 13 stations are abnormal. 10 stations appeared geo-sound anomalies,and 6 stations appeared electromagnetic disturbance anomalies. At the same time, a kind of electromagnetic disturbance waveform-SRSS wave,which is almost synchronous with sunrise and sunset,has been found. The waveform appears in many places around the epicenter. These anomalies may be the precursor anomalies of Jiuzhaigou earthquake. The AETA array successfully captures the precursory anomalies of multi-component and multi-station under a single earthquake case. In the future,it is proposed to increase the density of AETA array to do more in-depth research.

相似文献/References:

[1]梁厚朗,申 源,毛 利,等.芦山MS7.0与九寨沟MS7.0地震灾区房屋震害特征对比研究[J].华南地震,2019,39(03):14.[doi:10.13512/j.hndz.2019.03.003]
 LIANG Houlang,SHEN Yuan,MAO Li,et al.Comparison of Building Damage Characteristics of the Lushan MS7.0 and Jiuzhaigou MS7.0 Earthquakes[J].South China journal of seismology,2019,39(01):14.[doi:10.13512/j.hndz.2019.03.003]

备注/Memo

备注/Memo:
收稿日期:2018-10-22基金项目:深圳市科技计划(编号KJYY20170721151955849 & JCYJ20170412151159461)资助作者简介:王新安(1963- ),男,教授,主要从事地震监测预测和生命健康等研究. E-mail:anxinwang@pku.edu.cn.通信作者:雍珊珊(1987- ),博士,助理研究员,主要从事地震监测预测研究. E-mail:yongss@pkusz.edu.cn.
更新日期/Last Update: 2020-04-18