Fig. 1From: Provenance of upper Permian-lowermost Triassic sandstones, Wutonggou low-order cycle, Bogda Mountains, NW China: implications on the unroofing history of the Eastern North Tianshan SutureTectonic map of the Central Asian Orogenic Belt, which is bordered by the East European Craton to the west, Siberia Craton to the east, and North China, Tarim, and Karakum cratons to the south. Modified from Şengör et al. (1993) and Jahn et al. (2000). The Yellow box is the location of Fig. 2Back to article page