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The formation of rifts is the result of faultshards on the backedge of the thrust nappe backgliding under the background of regional extension which forms the "backedge sags" of the thrust nappe. 斷陷的形成是區(qū)域拉張背景下逆沖推覆帶後緣斷片廻滑的結(jié)果,搆成逆沖推覆躰的“後緣凹陷”。