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 uplift
Xiaomin Fang(Chinese Academy of Sciences), Shibo Tuo(Lanzhou University), Jinbo Zan(Chinese Academy of Sciences), Shuang Dai(Lanzhou University), Chunhui Song(Lanzhou University), Erwin Appel(University of Tübingen), Yin Lu(Chinese Academy of Sciences)
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