Pliocene-Pleistocene Climate Change At the NE Tibetan Plateau Deduced From Lithofacies Variation In the Drill Core SG-1, Western Qaidam Basin, China

Journal of Sedimentary Research - Tập 82 Số 12 - Trang 933-952 - 2012
Jiuyi Wang1, Xiaomin Fang1,2, Erwin Appel3, Song Chunhui4
1Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China
2School of Earth Sciences & Key Laboratory of Western China's Environmental Systems (MOE), Lanzhou University, Lanzhou 730000, China
3Department of Geoscience, University Tübingen, Hölderlinstrasse tu12, 72074 Tübingen, Germany e-mail:
4School of Earth Sciences and Key Laboratory of Western China's Environmental Systems (MOE), Lanzhou University, Lanzhou 730000, China

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Journal of Sedimentary Research

Tập 82 Số 12

933-952

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