简介:KazkeaertefaultzoneisrecognizedasanimportantboundarybetweenPamirandTianshanCenozoicMountainbeltsinthewestofTarimBasin.Itisanactivethrustfaultandcanbedividedintothreesegmentsfromthewesttoeast:Jilekeroutefaultzone,Wuqiaearthquakefaultzone,MushifaultzoneaftergeologicalinvestigatingandmappingalongPamirpiedmont.Basedonthefaultedlandformaswellasdeformationanddisplacementofyoungdepositlayers,theslipratesofKazkeaertefaultzonesincethelateQuaternaryarebrieflystudied.Theresultshowsthattheaveragesliprateoffaultisdifferentiatealongdifferentsegments.