Cenozoic magnetostratigraphy of the Xining Basin, NE Tibetan Plateau, and its constraints on paleontological, sedimentological and tectonomorphological evolutionXiaomin Fang, Tao Zhang, Qingquan Meng et al.|Earth-Science Reviews|2019Cited by 138
Tectonosedimentary evolution model of an intracontinental flexural (foreland) basin for paleoclimatic researchXiaomin Fang, Yin Lu, Maodu Yan et al.|Global and Planetary Change|2016Cited by 110
An Eocene–Miocene continuous rock magnetic record from the sediments in the Xining Basin, NW China: indication for Cenozoic persistent drying driven by global cooling and Tibetan Plateau upliftXiaomin Fang, Shibo Tuo, Jinbo Zan et al.|Geophysical Journal International|2015Cited by 90
Lithologic and rock magnetic evidence for the Mid-Miocene Climatic Optimum recorded in the sedimentary archive of the Xining Basin, NE Tibetan PlateauJinbo Zan, Yin Lu, Maodu Yan et al.|Palaeogeography Palaeoclimatology Palaeoecology|2015Cited by 44