摘要
ThedeformationpatternndHoloceneslipratealongtheFukangfaultinEasternTianshan,Chinaareanalyzedandstudiedusingthedataobtainedinfieldinvestigation.TheresultindicatesthattheFukangfaultconsistsof4low-anglesouth-dippingthrustfaultswithstepover,displayingrecenttectonicactivity.Themovementalongtheterminationpartsofthefaultisweaker,withanaverageverticalsliprateof0.13-0.33mm/ainHolocene,andalongthemiddlepartofthefaultisstronger,withanaverageverticalslipratelargerthan1.42mm/ainHolocene.TheHolocenedeformationpatternalongthefaultdisplaysgenerallysteadyslip,multi-phaseintermittentmovementalongitswesternsegment,andpersistentmovementalongitsmiddleandeasternsegments.whichhavecausedrapiddislocationuptothesurfaceinanearlierphase.
出版日期
2002年04月14日(中国期刊网平台首次上网日期,不代表论文的发表时间)