An Eocene-Miocene continuous high resolution 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

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ADS bibcode
2013AGUFM.T31B2515Z
year
2013
Listed Authors
Zan, J.
Fang, X.
Appel, E.
Yan, M.
Song, C.
Listed Institutions
ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;
ITP Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China;
Department of Geosciences, University of Tübingen, Tübingen, Germany;
Department of Geosciences, University of Tübingen, Tübingen, Germany;
School of Earth Sciences & Key Laboratory of Western China's Environmental Systems (MOE), Lanzhou University, Lanzhou, China;

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