Dynamic Magma Chamber Gas Escape and Recharge at Axial Seamount Revealed by Time‑Lapse Receiver Function Monitoring
Dynamic Magma Chamber Gas Escape and Recharge at Axial Seamount Revealed by Time‑Lapse Receiver Function Monitoring
Chang Gong1,2, Ruijia Wang2, Ling Chen3,4, Junlin Hua5,6, Sebastian Hainzl7,8, Christian Huber9, Mohammadreza Jamalreyhani10 and Zeyu Zhao11, (1)University of Science and Technology of China, Laboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, HeFei, China, (2)Southern University of Science and Technology, Department of Earth and Space Sciences, ShenZhen, China, (3)Institute of Geology and Geophysics, Chinese Academy of Sciences, State Key Laboratory of Lithospheric and Environmental Coevolution, Beijing, China, (4)College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China, (5)University of Science and Technology of China, Laboratory of Seismology and Physics of Earth’s Interior, School of Earth and Space Sciences, Hefei, China, (6)University of Science and Technology of China, State Key Laboratory of Precision Geodesy, HeFei, China, (7)GFZ Helmholtz Centre for Geosciences, Potsdam, Germany, (8)Institute for Geosciences, University of Potsdam, Potsdam-Golm, Germany, (9)Brown University, Department of Earth, Environmental and Planetary Sciences, Providence, RI, United States, (10)Southern University of Science and Technology, Department of Earth and Space Sciences, Shenzhen, Guangdong, China, (11)Peking University, School of Earth and Space Sciences, Beijing, China