摘要
盖州震群自2012年2月2日开始活动,截至2016年12月已活动了近5年的时间,其中持续活动的青石岭序列精定位后的空间展布在5km以内,深度也较为集中,可作为重复地震进行研究。通过计算盖州地区2012年2月—2016年12月M_L≥2.0重复地震序列经射线追踪法校正后的P波走时差,得到了盖州震群区域至岫岩台、辽阳台、高升台、瓦房店台四象限的介质变化情况,结果介质短期的变化受震群本身显著事件活动影响较为明显。中强地震前后周边地区介质变化显著。
By the time of December 2016 Gaizhou earthquake swarm activities has been lasted for nearly 5 years. The spatial distribution of the Qingshiling sequence of the continuous activity is within 5 km. The depth is also more concentrated and can be used as the study of recurrent earthquakes. Through the calculation of Gaizhou area M_L≥ 2.0 recurrent seismic sequence from February, 2012 to December, 2016 by ray tracing method after correction of P wave travel time difference, the four quadrant medium changes from Gaizhou earthquake swarm to Xiuyan Seismic Station, Liaoyang Seismic Station, Wafangdian Seismic Station. The results showed that the short-term change of media is obviously influenced by the events of the earthquake swarm itself. Before and after medium strong earthquake, the surrounding area has significant changed.
引文
[1]Poupinet G,Ellsworth W L,Frechet J.Monitoring Velocity Variations in the Crust Using Earthquake Doublets:An Application to the Calaveras Fault,California[J].J Geophys Res,1984,89(B7):5719-5731.
[2]周龙泉,刘桂萍,马宏生,等.利用重复地震观测地壳介质变化[J].地震,2007,27(3):l-9.
[3]叶秀薇,闻则刚,刘锦,等.利用重复地震研究广东阳江地区介质变化[J].地震,2008,28(4):103-111.
[4]李志伟,胥颐,郝天珧,等.环渤海地区的地震层析成像与地壳上地幔结构[J].地球物理学报,2006,49(3):797-804.