Stable isotope evidence for the Cenozoic paleoclimate evolution of the Hexi Corridor, Northern Tibetan Plateau

Fabiana Richter1, Carmala N Garzione1, Weitao Wang2, Jibao Dong3 and Feng Cheng4, (1)University of Rochester, Department of Earth and Environmental Sciences, Rochester, NY, United States, (2)China earthquake Bureau, Beijing, China, (3)Chinese Academy of Sciences, Institute of Earth Environment, Xi'an, China, (4)University of Rochester, Department of Earth and Environmental Sciences, Rochester, United States
Back to: Growth of the Himalayan-Tibetan Plateau: Timing, Geodynamic Drivers, and Climatic Effects Posters