*Tatsuya Hattori1,2, Ryosuke Oyanagi4,5, Tomoyuki Mizukami1, Yumiko Harigane6, Mayuko Fukuyama7, Asuka Yamaguchi8, Tomoaki Morishita1,3
(1. School of Geosciences and Civil Engineering, Kanazawa University, 2. Geology and Geophysics Division, Japan Organization for Metals and Energy Security (JOGMEC), 3. Volcanoes and Earth’s Interior Research Center, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 4. School of Engineering and Science, Kokushikan University, 5. Research Institute for Marine Geodynamics, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), 6. Institute of Geology and Geoinformation, Geological Survey of Japan, AIST, 7. Graduate School of Engineering Science, Akita University, 8. Atmosphere and Ocean Research Institute, The University of Tokyo)
Keywords:Carbonation, Ultramafic rocks, Clinopyroxenite, Izu-Bonin-Mariana arc