Activity Feature of Kazkeaerte Fault Zone in the Late Quaternary-中国期刊网

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

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Activity Feature of Kazkeaerte Fault Zone in the Late Quaternary

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Activity Feature of Kazkeaerte Fault Zone in the Late Quaternary

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