A New Method for Determining Fluid Flux at High Pressures Applied to the Dehydration of Serpentinites

A New Method for Determining Fluid Flux at High Pressures Applied to the Dehydration of Serpentinites

Abstract A new method to determine fluid flux at high pressures and temperatures has been developed and used to study serpentinites at subduction zone conditions. Drill cores of a natural antigorite‐serpentinite with a strong foliation were used in multi‐anvil experiments in the range of 2–5 GPa and...

Täydet tiedot

Bibliografiset tiedot
Päätekijät: L. Eberhard, M. Thielmann, P. Eichheimer, A. Néri, A. Suzuki, M. Ohl, W. Fujita, K. Uesugi, M. Nakamura, G. J. Golabek, D. J. Frost
Aineistotyyppi: Artikkeli
Kieli:English
Julkaistu: Wiley 2022-09-01
Sarja:Geochemistry, Geophysics, Geosystems
Aiheet:
fluid flux
multi‐anvil
serpentine
brucite
dehydration
excess pressure
Linkit:https://doi.org/10.1029/2021GC010062

Internet

https://doi.org/10.1029/2021GC010062

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