简介：ShearwavesplittingisstudiedbasedonthedigitalwaveformsofthreeseismicstationsDJS,SZDandWUJ,whichweresetupaftertheJiujiang-RuichangMS5.7earthquakeofNovember26,2005aroundtheepicenterarea.TheresultshowsthatthetimedelaysofslowshearwavesoftheDJSstation,whichisnotfarfromtheepicenterandwherethedistributionoffaultsiscomplexnearthestation,arerelativelylargerandthepolarizationdirectionsoffastshearwavesarenotconcentrated;thepredominantpolarizationdirectionoffastshearwavesofWUJstation,withsinglefaultdistributednearby,hasadifferenceof35°tothestrikeofthefaultandisinconsistentwiththedirectionofregionalprincipalcompressivestress.ThepredominantpolarizationdirectionoffastshearwavesofSZDstationwithnofaultsnearbyisinaccordancewithregionalprincipalcompressivestress.Thereisnoobviousregularrelationshipshipbetweenthedelaytimeandthefocaldepth.