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...
Huvudupphovsmän: | Tian, M, Katz, R, Rees Jones, D, May, D |
---|---|
Materialtyp: | Journal article |
Språk: | English |
Publicerad: |
American Geophysical Union
2019
|
Liknande verk
Liknande verk
-
Devolatilization of subducting slabs, Part I: Thermodynamic parameterization and open system effects
av: Tian, M, et al.
Publicerad: (2019) -
Pervasive subduction zone devolatilization recycles CO2 into the forearc
av: E. M. Stewart, et al.
Publicerad: (2020-12-01) -
Kimberlite eruptions driven by slab flux and subduction angle
av: Ben R. Mather, et al.
Publicerad: (2023-06-01) -
Halogen (F, Cl, Br, and I) Devolatilization During Prograde Subduction: Insights From Western Alps Ophiolites
av: G. M. Beaudoin, et al.
Publicerad: (2024-04-01) -
Covariation of Slab Tracers, Volatiles, and Oxidation During Subduction Initiation
av: Maryjo Brounce, et al.
Publicerad: (2021-06-01)