Nature Communications (Jul 2021)
Linking deeply-sourced volatile emissions to plateau growth dynamics in southeastern Tibetan Plateau
- Maoliang Zhang,
- Zhengfu Guo,
- Sheng Xu,
- Peter H. Barry,
- Yuji Sano,
- Lihong Zhang,
- Sæmundur A. Halldórsson,
- Ai-Ti Chen,
- Zhihui Cheng,
- Cong-Qiang Liu,
- Si-Liang Li,
- Yun-Chao Lang,
- Guodong Zheng,
- Zhongping Li,
- Liwu Li,
- Ying Li
Affiliations
- Maoliang Zhang
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Zhengfu Guo
- Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS)
- Sheng Xu
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Peter H. Barry
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution
- Yuji Sano
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Lihong Zhang
- School of Geology and Geomatics, Tianjin Chengjian University
- Sæmundur A. Halldórsson
- NordVulk, Institute of Earth Sciences, University of Iceland
- Ai-Ti Chen
- Department of Geosciences, National Taiwan University
- Zhihui Cheng
- School of Earth Science and Engineering, Sun Yat-sen University
- Cong-Qiang Liu
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Si-Liang Li
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Yun-Chao Lang
- Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University
- Guodong Zheng
- Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Zhongping Li
- Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Liwu Li
- Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences
- Ying Li
- Institute of Earthquake Forecasting, China Earthquake Administration
- DOI
- https://doi.org/10.1038/s41467-021-24415-y
- Journal volume & issue
-
Vol. 12,
no. 1
pp. 1 – 10
Abstract
Deeply-sourced volatiles are releasing from orogenic plateau regions, providing windows to plateau growth dynamics occurring at variable depths. Here the authors show that mantle-derived volatiles reveal the involvement of mantle dynamics in southeastward growth of the Tibetan Plateau.
