A classical Mesozoic thrustbelt lies in the Longmen Mountain area along the western margin of the Yangtze massif, where Devonian strata are widespread and very thick and there are a variety of sediment types, including both the unmetamorphosed stable type
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刘文均,郑荣才,李祥辉.1999.龙门山泥盆纪沉积盆地的古地理和古构造重建[J].地质学报,73(2). Liu Wenjun, Zheng Rongcai, Li Xianghui.1999. Reconstruction of Palaeogeography and Palaeotectonics of a Devonian Sedimentary Basin in the Longmenshan Area, Sichuan[J]. Acta Geologica Sinica,73(2).