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作者单位: | Institute of Geological Survey, China University of Geosciences, Wuhan, 430074, China; State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China; CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla, 666303, China; School of Environment, Earth and Ecosystem Sciences, The Open University, Milton Keynes, MK7 6AA, United Kingdom; School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, United Kingdom; Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China; School of Earth Sciences, East China University of Technology, Nanchang, 330013, China; School of Earth Sciences, China University of Geosciences, Wuhan, 430074, China; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing, 210008, China
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Recommended Citation: |
Song B.,Spicer R.A.,Zhang K.,et al. Qaidam Basin leaf fossils show northeastern Tibet was high, wet and cool in the early Oligocene[J]. Earth and Planetary Science Letters,2020-01-01,537
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