北部湾6.1、6.2级地震的震源参数和Q_P值特征
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
利用中国数字地震台网(CDSN)琼中台短周期垂直向P波数字地震资料,研究了1994年12月北部湾6.1、6.2级地震的震源特征,并对震情趋势作出估计。研究表明,北部湾地震的余震应力降和介质QP值分别为3.65×105Pa和285,在震区附近发生更大地震的可能性不大;在东方小震群区,测定的应力降和介质QP值分别为1.65×105Pa和266,符合小震群震源特征;在琼东北地区,应力降不高,QP值为190;海南岛东南的陵水及其海域应力降也不高,QP值为480。这两个地区均存在着孕育较大地震的介质条件,特别是琼东北地区。
The source characteristics of the Ms6.1 and Ms6.2 earthquakes occurred in Beibuwan are studied by using digital seiSmic data of the short period vertical component of P wave,and the earthquake trend is also analyzied.The results show that the stress drop of the aftershocks of the Beibuwan earthquake and their QpValues are respectively about 3.65×105pa and 285.The possibility for occurring larger earthquake is not too large in and near the Beibuwan earthquake region.The determining stress drop andQpvalue are respectively about 1.65×105pa and 266 in the Dongfang small earthquake swarm reston,which are in agreement with the source characteriStics of the small earthquake swarm.The stress drop in northeast Qiong region is not too high and Qpvalue in this region is about 490;and that in Lingshui region and its sea area of southeast Hainan Island also and Qpvalue 480.The medium condictions of larger earthquake preparation exist in both districts,especially,in northeast Qiong region.
引文
1朱传镇,傅昌洪,容珍贵,罗胜利.海城地震前后微震震源参数和介质品质因子.地球物理学报,1977(3):222~2312朱传镇,傅昌洪,罗胜利.唐山7.8级地震前后微震震源参数.地球物理学报,1977(4):264~2693M.E.O'neillandJ.H.Healy,Determinationofsourceparametersofsmallearthquakesfromp-waverisetime,Bull.Seism.Soc.Am,1973,63(2).4J.N.Brune,Tectonicstressandthespectraofseismicshearwavesfromearthquake,J.Geophys.Res,1970,(75):4997~50095W.H.BakunandC.G.Bute,ShearwaveattenuationalongtheSanAndresfaultzoneincentralCalifornin,Bull.Seism.Soc.Am,1975,(65):439~4596郑治真.波谱分析基础.北京:地震出版社,1979.7朱传镇,傅昌洪,安镇文.海南岛及其邻区的小震应力降和介质Q值.见:丁原章等编.海南岛北部地震研究文集.北京:地震出版社,1988,227~2348傅昌洪.利用CDSN资料研究中强地震的差异.地震地磁观测与研究,1992,13(3):31~39

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心