The Napanjiang basin is tectonically located at the juncture of the Tethys and Pacific tectonic domain. In the Early Palaeozoic, as a part of the southeastern passive margin of the Yangtze Plate, had been involved in the Caledonian orogenic belt resulting
秦建华,吴应林,颜仰基,朱忠发.1996.南盘江盆地海西-印支期沉积构造演化[J].地质学报,70(2). Qin Jianhua, Wu Yinglin, Yan Yangji, Zu Zhongfa.1996. HERCYNIAN-INDOSINIAN SEDIMENTARY-TECTONIC EVOLUTION OF THE NANPANJIANG BASIN[J]. Acta Geologica Sinica,70(2).
