Devolatilization of subducting slabs, part II: volatile fluxes and storage
<p>Subduction is a crucial part of the long‐term water and carbon cycling between Earth's exosphere and interior. However, there is broad disagreement over how much water and carbon is liberated from subducting slabs to the mantle wedge and transported to island‐arc volcanoes. In the comp...
Principais autores: | Tian, M, Katz, R, Rees Jones, D, May, D |
---|---|
Formato: | Journal article |
Idioma: | English |
Publicado em: |
American Geophysical Union
2019
|
Registros relacionados
-
Devolatilization of subducting slabs, Part I: Thermodynamic parameterization and open system effects
por: Tian, M, et al.
Publicado em: (2019) -
Pervasive subduction zone devolatilization recycles CO2 into the forearc
por: E. M. Stewart, et al.
Publicado em: (2020-12-01) -
Kimberlite eruptions driven by slab flux and subduction angle
por: Ben R. Mather, et al.
Publicado em: (2023-06-01) -
Halogen (F, Cl, Br, and I) Devolatilization During Prograde Subduction: Insights From Western Alps Ophiolites
por: G. M. Beaudoin, et al.
Publicado em: (2024-04-01) -
Covariation of Slab Tracers, Volatiles, and Oxidation During Subduction Initiation
por: Maryjo Brounce, et al.
Publicado em: (2021-06-01)