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Deep carbon cycling during subduction revealed by coexisting diamond-methane-magnesite in peridotite.
Wang, Xiaoxia; Xiao, Yilin; Schertl, Hans-Peter; Sobolev, Nikolay V; Wang, Yang-Yang; Sun, He; Jin, Deshi; Tan, Dong-Bo.
Afiliação
  • Wang X; CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, China.
  • Xiao Y; CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, China.
  • Schertl HP; CAS Center for Excellence in Comparative Planetology, China.
  • Sobolev NV; Ruhr-University Bochum, Faculty of Geosciences, Institute of Geology, Mineralogy and Geophysics, Germany.
  • Wang YY; V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of Russian Academy of Sciences, Russia.
  • Sun H; CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, China.
  • Jin D; School of Resources and Environmental Engineering, Hefei University of Technology, China.
  • Tan DB; CAS Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, China.
Natl Sci Rev ; 10(10): nwad203, 2023 Oct.
Article em En | MEDLINE | ID: mdl-37671326
Identification of multiphase inclusions in peridotite suggests that released carbon from a subducting slab can be stored as diamond+methane+magnesite in the overlying mantle wedge, achieving deep carbon cycling.

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Natl Sci Rev Ano de publicação: 2023 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Revista: Natl Sci Rev Ano de publicação: 2023 Tipo de documento: Article