Center for High Pressure Science and Technology Advanced Research (HPSTAR), Beijing, China; Institute of Meteoritics, Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, United States; Key Laboratory of High-Temperature and High-Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China; Department of Chemistry, Pohang University of Science and Technology, Pohang, South Korea; College of New Materials and New Energies, Shenzhen Technology UniversityGuangdong, China; School of Materials Science and Engineering, Changchun University of Science and Technology, Changchun, China; Center for Study of Matter under Extreme Conditions, Department of Mechanical and Materials Engineering, Florida International University, Miami, FL, United States; Department of Geological Sciences, Stanford University, Stanford, CA, United States; High Pressure Collaborative Access Team, X-ray Science Division, Argonne National Laboratory, Argonne, IL, United States; Center for Advanced Radiation Sources, University of Chicago, Chicago, IL, United States; Department of Materials Science and Metallurgy, University of Cambridge, Cambridge, United Kingdom; Advanced Institute for Materials Research, Tohoku University, Aoba, Sendai, Japan; Theory of Condensed Matter Group, Cavendish Laboratory, Cambridge, United Kingdom
Recommended Citation:
Hou M.,He Y.,Jang B.G.,et al. Superionic iron oxide–hydroxide in Earth’s deep mantle[J]. Nature Geoscience,2021-01-01,14(3)