[M-IS04] Paleoclimatology and paleoceanography

[MIS04-21] Intensified silicate weathering linked to tectonic uplift on the northern Tibetan Plateau during the middle–late Miocene

*YU LIANG^1,2, David B. Kemp³, Zhonghui Liu^4,10, Zerui Ray Liu², Hitoshi Hasegawa⁵, Bailong Liu⁶, Bin Zhang⁷, Yongshu Zhang⁸, Mei-Fu Zhou^9,2 (1. Marine Core Research Institute, Kochi University, 2. State Key Laboratory of Geological Processes and Mineral Resources, School of Earth Resources, China University of Geosciences, 3. State Key Laboratory of Geomicrobiology and Environmental Changes and Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences, 4. Department of Earth and Planetary Sciences, The University of Hong Kong, 5. Faculty of Science and Technology, Kochi University, 6. State Key Laboratory of Continental Shale Oil, China National Petroleum Corporation, 7. Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, 8. Qinghai Oilfield, China National Petroleum Corporation, 9. State Key Laboratory of Laboratory of Critical Mineral Research and Exploration, Institute of Geochemistry, Chinese Academy of Sciences, 10. Institute for Climate and Carbon Neutrality, The University of Hong Kong)

Keywords:Northern Tibetan Plateau, Middle-late Miocene, Tectonic uplift, Silicate weathering, Lithium isotope