首页 | 本学科首页   官方微博 | 高级检索  
     

2020年古冶MS5.1地震序列微震检测及活动性研究
引用本文:王同利, 张盛中, 崔博闻, 武敏捷, 马泽宇, 葛慧颖. 2024. 2020年古冶MS5.1地震序列微震检测及活动性研究. 地球物理学报, 67(4): 1501-1514, doi: 10.6038/cjg2023Q0865
作者姓名:王同利  张盛中  崔博闻  武敏捷  马泽宇  葛慧颖
作者单位:1. 北京市地震局, 北京 100081; 2. 中国地质大学(北京)信息网络与数据中心, 北京 100083; 3. 中国地质大学(北京)地球物理与信息技术学院, 北京 100083
基金项目:北京市自然科学基金项目(8212041)资助
摘    要:

2020年7月12日河北省古冶(39.78°N, 118.44°E)发生MS5.1地震, 震源深度10 km.本文通过对其周边500 km范围内的84个固定台站连续观测地震数据, 采用基于图形处理器的模板匹配定位识别技术(GPU-M&L)对地震前后(2020年6月1日至2020年8月31日)共三个月的连续数据进行了微震检测和地震活动性分析.我们首先从台网目录的362个古冶地震序列事件中挑选了信噪比较高的118个地震作为模板, 通过模板扫描和检测, 获得共1017个地震, 约为台网目录的2.8倍, 然后运用双差定位方法(hypoDD)对669个地震事件进行了重定位.
最后我们对古冶地震的事件序列进行时空分布、震源机制解以及b值空间分布等分析.结果显示古冶MS5.1地震前, 震中区周边地震活动性显著, 地震前后地震序列分布优势方向为NE向, 震源深度方向近直立分布; 发震断裂为唐山—古冶断裂或其延伸部分, 与1976年唐山MS7.8地震同为唐山断裂带, 发震断层走向基本一致.据此, 我们推测古冶MS5.1地震是1976年唐山MS7.8地震后余震区应力调整所触发.




关 键 词:古冶地震   微震检测   模板匹配   完备震级   地震活动性
收稿时间:2022-10-25
修稿时间:2023-11-13

Microearthquake detection and seismicity analysis of the 2020 Guye MS5.1 earthquake sequence
WANG TongLi, ZHANG ShengZhong, CUI BoWen, WU MinJie, MA ZeYu, GE HuiYing. 2024. Microearthquake detection and seismicity analysis of the 2020 Guye MS5.1 earthquake sequence. Chinese Journal of Geophysics (in Chinese), 67(4): 1501-1514, doi: 10.6038/cjg2023Q0865
Authors:WANG TongLi  ZHANG ShengZhong  CUI BoWen  WU MinJie  MA ZeYu  GE HuiYing
Affiliation:1. Beijing Earthquake Agency, Beijing 100081, China; 2. Information Network and Data Center, China University of Geosciences, Beijing 100083, China; 3. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
Abstract:
On July 12, 2020, a MS5.1 earthquake (epicenter: 39.78°N, 118.44°E) with a depth of ~10 km struck Guye, Tangshan, Hebei province. In this paper, we performed microearthquake detection and seismicity analysis using the three-month continuous waveform data (from June 1, 2020 to August 31, 2020) recorded by 84 stations within 500 km radius around the epicenter. Firstly, we selected 118 high-quality events as templates from 362 events listed in the China Earthquake Network Center (CENC) catalog. By scanning through the three-month continuous data using the Graphic Processing Unit based Match and Locate (GPU-M&L) technique, a total of 1017 events were detected, which is approximately 2.8 times the number in the CENC catalog.
Secondly, 669 earthquakes were relocated by applying the double difference relocation algorithm (hypoDD). We then analyzed the temporal-spatial distribution, focal mechanism solutions, and spatial variation of the b-value for the Guye earthquake sequence. Our results reveal that the Guye MS5.1 earthquake sequence exhibits a NE-striking pattern on the surface and a subvertical distribution in depth, which is spatially coincident with the eastward extension of the Tangshan-Guye Fault. Since both the seismogenic faults of the Guye MS5.1 earthquake and the 1976 MS7.8 Tangshan earthquake belong to the Tangshan fault system, we suggest that the Guye earthquake was triggered by stress adjustment of the Tangshan MS7.8 earthquake.
Keywords:The Guye earthquake  Microseismic detection  Template matching  The magnitude of completeness  Seismicity
点击此处可从《地球物理学报》浏览原始摘要信息
点击此处可从《地球物理学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号