岫岩地震序列视应力变化及其预测意义
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摘要
选取辽宁省地震局沈阳数字化地震台网中的岫岩、营口、本溪、北镇、新民5个台的波形记录, 计算了1999年11月29日岫岩MS5.4地震序列视应力值。5 个台资料的计算结果具有很好的一致性, 即岫岩序列的视应力变化特征具有显著的共性特征: 震前低视应力阶段、震时高视应力阶段和震后逐渐降低的调整至稳定阶段, MS5.4 主震和5.1 级最大强余震前视应力升高, 表明视应力可作为中强震及震后地震趋势预测的判定依据。
the authors use waveform records of 5 stations of Xiuyan, Yingkou, Benxi, Beizhen and Xinmin from digital seismic station network of Shenyang, Earthquake Administration of Liaoning Province, to calculate apparent stress of Xiuyan sequence of M_S5.4 earthquake occurred on Nov. 29, 1999. The calculated results from the five stations are well consistent, and change of apparent stress of Xiuyan sequence has notable common feature, i.e. low apparent stress phase before earthquake, high apparent stress phase while earthquake occurrence and adjusting and stable phase after earthquake, during this phase, the stress reduced gradually. That apparent stress increase before the M_S5.4 mainshock and maximum strong aftershocks of M_S5.1 show that apparent stress could be regarded as criterion of earthquake tendency before and after moderately strong earthquakes.
the authors use waveform records of 5 stations of Xiuyan, Yingkou, Benxi, Beizhen and Xinmin from digital seismic station network of Shenyang, Earthquake Administration of Liaoning Province, to calculate apparent stress of Xiuyan sequence of M_S5.4 earthquake occurred on Nov. 29, 1999. The calculated results from the five stations are well consistent, and change of apparent stress of Xiuyan sequence has notable common feature, i.e. low apparent stress phase before earthquake, high apparent stress phase while earthquake occurrence and adjusting and stable phase after earthquake, during this phase, the stress reduced gradually. That apparent stress increase before the M_S5.4 mainshock and maximum strong aftershocks of M_S5.1 show that apparent stress could be regarded as criterion of earthquake tendency before and after moderately strong earthquakes.
引文
[1] 中国地震局监测预报司.地震参数数字地震学在地震预测中的应用[M].北京:地震出版社,2003.
[2] 吴忠良,黄静,林碧苍.中国西部地震视应力的空间分布[J].地震学报,2002,24(3):293301.
[3] 陈学忠,王小平,王林瑛,等.地震视应力用于震后趋势快速判定的可能性[J].国际地震动态,2003,7(295):14.
[4] 吴忠良.由宽频带辐射能量目录和地震矩目录给出的视应力及其地震学意义[J].中国地震,2001,17(1):815.
[5] WyssM,BruneJ N.Seismic moment, stress, and source dimensions for earthquakes in theCalifor niaNevada region[J].J GeophysRes,1968,73:46814694.
[6] AndrewsD J.Objective determination of source parameters and similarity of earthquakes of differentsize[A].In:DasS,BoatwrightJ,ScholzC H (eds.).Earthquake sourceMechanics[C].Washing ton,D.C.:AGU,1986,259267.
[7] 孙文福,焦明若.1999年岫岩5.6级地震序列活动跟踪研究[J].东北地震研究,2001,17(2):816.
[2] 吴忠良,黄静,林碧苍.中国西部地震视应力的空间分布[J].地震学报,2002,24(3):293301.
[3] 陈学忠,王小平,王林瑛,等.地震视应力用于震后趋势快速判定的可能性[J].国际地震动态,2003,7(295):14.
[4] 吴忠良.由宽频带辐射能量目录和地震矩目录给出的视应力及其地震学意义[J].中国地震,2001,17(1):815.
[5] WyssM,BruneJ N.Seismic moment, stress, and source dimensions for earthquakes in theCalifor niaNevada region[J].J GeophysRes,1968,73:46814694.
[6] AndrewsD J.Objective determination of source parameters and similarity of earthquakes of differentsize[A].In:DasS,BoatwrightJ,ScholzC H (eds.).Earthquake sourceMechanics[C].Washing ton,D.C.:AGU,1986,259267.
[7] 孙文福,焦明若.1999年岫岩5.6级地震序列活动跟踪研究[J].东北地震研究,2001,17(2):816.
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