岫岩M_S5.4地震前后S波分裂研究  

STUDY ON S-WAVE FISSION AROUND XIUYAN M_S5.4 EARTHQUAKE

作　　者：曹凤娟[1] 王连权[1] 张萍[1] 迮安民[2] 刘友富[1] 

机构地区：[1]辽宁省地震局,辽宁沈阳110031 [2]丹东地震台,辽宁丹东118000

出　　处：《东北地震研究》2005年第4期39-44,共6页Seismological Research of Northeast China

基　　金：中国地震局"数字化实验室"的部分研究成果

摘　　要：利用辽宁数字地震台网的营口台的三分向数字化地震资料,研究了1999年岫岩MS5.4地震前后S波分裂特征。结果表明:(1)延迟时间大部分在0.9~7.2ms/km范围内,平均4.23ms/km;(2)震前快S波的优势偏振方向为N51°~88°E,平均N58.66°E;震后S波的偏振方向主要集中在N1°W^N2°E和N55°~84°E范围内,平均偏振角为近NS向和N68.13°E。NE的偏振方向与震源应力场的主压应力方向N70°E接近,由此推测1999年岫岩MS5.4地震的S波分裂是震源应力场引起的介质各向异性的结果。The characteristics of S -wave fission around Xiuyan Ms5.4 eartquake in 1999 are studied by using 3D digital earthquake data of Yingkou station in Liaoning digital earthquake network. The results show： ①Delay time of most earthquakes is from 0.9ms/km to 7.2ms/km and the average is 4.23ms/ km; ②Before the earthquake, the polarization direction of fast S - wave is from N51° to 88° E and the average is N58.66° E; After the earthquake, the polarization direction of fast S-wave is concentrated on N1W°-N2° E and N55°-84°E, the average is NS and N68.13° E. And the NE polarization direction is closed to N70°E which is the principal pressure stress direction in this focal stress field. So, it is deduced that the S - wave fission of Xiuyan Ms5.4 earthquake in 1999 is the result of medium anisotropy caused by the focal stress field.

关 键 词：岫岩Ms5.4地震 S波分裂 主压应力 延迟时间 各向异性 

分 类 号：P315.7[天文地球—地震学] P315.3[天文地球—固体地球物理学]