Cargando…
Massive abiotic methane production in eclogite during cold subduction
Methane (CH(4)) is a critical but overlooked component in the study of the deep carbon cycle. Abiotic CH(4) produced by serpentinization of ultramafic rocks has received extensive attention, but its formation and flux in mafic rocks during subduction remain poorly understood. Here, we report massive...
Autores principales: | Zhang, Lijuan, Zhang, Lifei, Tang, Ming, Wang, Xiao, Tao, Renbiao, Xu, Cheng, Bader, Thomas |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Oxford University Press
2022
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9840456/ https://www.ncbi.nlm.nih.gov/pubmed/36654916 http://dx.doi.org/10.1093/nsr/nwac207 |
Ejemplares similares
-
Massive production of abiotic methane during subduction evidenced in metamorphosed ophicarbonates from the Italian Alps
por: Vitale Brovarone, Alberto, et al.
Publicado: (2017) -
Cold deep subduction recorded by remnants of a Paleoproterozoic carbonated slab
por: Xu, Cheng, et al.
Publicado: (2018) -
Partial melting of deeply subducted eclogite from the Sulu orogen in China
por: Wang, Lu, et al.
Publicado: (2014) -
Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite
por: Aulbach, Sonja, et al.
Publicado: (2022) -
The role of continental subduction in mantle metasomatism and carbon recycling revealed by melt inclusions in UHP eclogites
por: Borghini, Alessia, et al.
Publicado: (2023)