The arcuate nappe structure on the northern margin of the Wuliang Mountains in western Yunnan is a complex nappe system with multiple superimposed structures. The autochthonous system is a WNW-vergent arcuate fold belt formed by Jurassic-Creaceous red bed
李述靖 单业华.1995.滇西无量山北缘弧形推覆构造[J].地质学报,69(4). Li Shujin, Shan Yehua.1995. ARCUATE NAPPE STRUCTURE ON THE NORTHERN MARGIN OF THE WULIANG MOUNTAINS IN WESTERN YUNNAN[J]. Acta Geologica Sinica,69(4).
