以河北测震台网记录的连续波形数据为基础,采用模板匹配滤波方法,检测2017年9月4日-6日河北临城震群遗漏地震。利用波形互相关扫描,检测到19次被测震台网常规分析遗漏的地震,震级范围为ML 0.0-1.2,并标定新检测地震事件的P波和S波到时,估计其震中位置及震级。通过地震精定位和最大地震震源机制解,认为此次临城地震序列的主要发震构造应为近EW向活动断层。
Based on the continuous wave data recorded by Hebei Digital Seismic Network, this paper uses the template matching filtering method to detect the missing earthquakes of the Lincheng earthquake swarm in Hebei from September 4th to 6th, 2017. Using the waveform cross-correlation technique, 19 missing earthquakes that were routinely analyzed by the seismic network were detected. The magnitude range was ML 0.0-1.2, and the P-and S-wave arrivals of the newly detected seismic events were estimated, and the epicenter location and magnitude were estimated.Through relocation result and earthquake mechanism of maximum earthquake.We analyze that the main seismogenic structure of the Lincheng earthquake swarm may be the near EW active fault.
2019,40(6): 9-14 收稿日期:2019-03-27
DOI:10.3969/j.issn.1003-3246.2019.06.002
基金项目:中国地震局监测预报司测震台网青年骨干专项(项目编号:CEA-JC/QNCZ-18041);河北省地震局星火计划(项目编号:DZ20190422038);中国地震局震情跟踪课题(项目编号:2019010105)
作者简介:王宁(1988-),女,河北邯郸人,工程师,主要从事地震监测研究工作。E-mail:819087955@qq.com
参考文献:
蔡玲玲,李冬圣,孟立朋,等. 京西北地区地震重定位分析[J]. 地震地磁观测与研究,2017,38(3):47-52.
李璐. 台阵处理和模板匹配滤波技术在微弱地震信号检测中的应用研究[D]. 北京:中国地震局地球物理研究所,2016.
谭毅培,曹井泉,卞真付,等. 2013年8月河北蔚县小震群遗漏地震检测与发震构造分析[J]. 地震学报,2014,36(6):1 022-1 031.
谭毅培,曹井泉,刘文兵,等. 2013年3月涿鹿微震群遗漏地震事件检测和发震构造分析[J]. 地球物理学报,2014,57(6):1 847-1 856.
王宁,杨春利,李雪英,等. 遗漏震相检测技术在2016年9月唐山震群中的应用[J]. 华北地震科学,2017,35(1):38-43.
徐杰,方仲景. 1966年邢台7.2级地震的构造背景和发震构造[J]. 地震地质,1988,10(4):51-59.
Gibbons S J, Ringdal F. The detection of low magnitude seismic events using array-based waveform correlation[J]. Geophys J Int, 2006, 165(1):149-166.
Peng Z G, Zhao P. Migration of early aftershocks following the 2004 Parkfield earthquake[J]. Nature Geoscience, 2009, 2(12):877-881.
Shally D R, Beroza G C, Ide S. Non-volcanic tremor and low-frequency earthquake swarms[J]. Nature, 2007, 446(7 133):305-307.
Yao D D, Peng Z G, Meng X F. Remotely triggered earthquakes in South-Central Tibet following the 2004 MW 9.1 Sumatra and 2005 MW 8.6 Nias earthquakes[J]. Geophys J Int, 2015, 201(2):543-551.