The Cenozoic Kuqa foreland fold-and-thrust belt in Xinjiang could be divided,in southward order,into the basement thrusting belt,box anticline belt,comb anticline belt and bended folding belt And along the W-E orientation,it could be divided into the western,middle and eastern segnents The paper described deformation features of each segment,and thought that the deformation became weakened and the topographic relief tended to planation eastwards since the box anticline belt being not developed in the easter...
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