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