Deep carbon cycling during subduction revealed by coexisting diamond-methane-magnesite in peridotite

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.

Detalles Bibliográficos
Autores principales: Wang, Xiaoxia, Xiao, Yilin, Schertl, Hans-Peter, Sobolev, Nikolay V, Wang, Yang-Yang, Sun, He, Jin, Deshi, Tan, Dong-Bo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2023
Materias:
Perspective
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10476885/
https://www.ncbi.nlm.nih.gov/pubmed/37671326
http://dx.doi.org/10.1093/nsr/nwad203

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10476885/
https://www.ncbi.nlm.nih.gov/pubmed/37671326
http://dx.doi.org/10.1093/nsr/nwad203

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