Deformation Pattern and Holocene Slip Rate Along the Fukang Fault in Eastern Tianshan,China

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摘要 ThedeformationpatternndHoloceneslipratealongtheFukangfaultinEasternTianshan,Chinaareanalyzedandstudiedusingthedataobtainedinfieldinvestigation.TheresultindicatesthattheFukangfaultconsistsof4low-anglesouth-dippingthrustfaultswithstepover,displayingrecenttectonicactivity.Themovementalongtheterminationpartsofthefaultisweaker,withanaverageverticalsliprateof0.13-0.33mm/ainHolocene,andalongthemiddlepartofthefaultisstronger,withanaverageverticalslipratelargerthan1.42mm/ainHolocene.TheHolocenedeformationpatternalongthefaultdisplaysgenerallysteadyslip,multi-phaseintermittentmovementalongitswesternsegment,andpersistentmovementalongitsmiddleandeasternsegments.whichhavecausedrapiddislocationuptothesurfaceinanearlierphase.
机构地区 不详
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)
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