腾冲地震台数字地震记录S波分裂研究
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摘要
对2000~2010年腾冲地震台数字地震资料进行S波分裂研究,得到了腾冲地区不同时间段内的应力优势方向和S波延迟时间。结果表明,其快波偏振方向主要集中在NE30°~55°,这与该区的主应力场方向基本一致。横波分裂延迟时间能为地震预报和区域应力场研究提供有用的信息。
Using the digital data from 2002 to 2010 recorded by Tengchong Seismic Station,we conducted a shear wave splitting and obtained the predominant direction of stress and the delay time of shear wave in different stages from 2002 to 2010 in Tengchong.Further,we found that the predominant polarization direction was in NE30°-55°,agreeing with the one of the regional principal compressive stress.The delay time of the shear wave provides useful information for the study of the regional stress field and the earthquakes prediction.
引文
贺传松,王春镛,吴建平,等.2004.腾冲火山区S波速度结构接受函数反演[J].地震学报,26(1):11-18.
    贺曼秋,魏红梅,章静,等.2008.荣昌台S波分裂研究[J].内陆地震,22(1):84-87.
    姜朝松,王绍晋,叶建庆,等.2005.腾冲火山区小震震源机制解特征[J].地震研究,28(2):141-143.
    毛慧玲,秦嘉政.2011.2007年宁洱6.4级地震横波分裂研究[J].地震研究,34(1):42-46.
    秦嘉政,皇甫岗,张俊伟,等.1998.腾冲火山及其周围地区的地壳Q值特征[J].地震研究,21(4):358-361.
    钱晓东,秦嘉政.2000.云南腾冲火山地区的地震类型[J].四川地震,(3):43-48.
    王椿镛,皇甫岗,万登堡,等.2000.腾冲火山区地壳结构的人工地震探测[J].地震研究,23(2):148-156.
    Crampin S,Atkinson B k.1985.Microcracks in the Earth's crust[J].First Break,3(3):16-20.
    Crampin S,Volti T,Stefansson R.1999.A successfully stress-forecast earthquake[J].Geopys J Int,138(1):F1-F5.
    Crampin S,Zatsepin S V.1997.Modelling the compliance of crustal rock-II.Response to temporal changes before earthquakes[J].Geophys J Int,129(3):495-506.
    Garbin H D,Knopoff L.1975.The shear modulus of a material permeated by a random distribution of circular cracks[J].Q Appl Math,33:296-300.

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