JOURNAL OF ASIAN EARTH SCIENCES, cilt.108, ss.117-135, 2015 (SCI İndekslerine Giren Dergi)
The chronostratigraphy of Guandao section has served as the foundation for numerous studies of the end-Permian extinction and biotic recovery in south China. Guandao section is continuous from the Permian-Triassic boundary to the Upper Triassic.