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On the Influence of Pressure, Phase Transitions, and Water on Large‐Scale Seismic Anisotropy Underneath a Subduction Zone

Abstract Seismic anisotropy mainly originates from the crystallographic preferred orientation (CPO) of minerals deformed in the convective mantle flow. While fabric transitions have been previously observed in experiments, their influence on large‐scale anisotropy is not well‐documented. Here, we im...

Deskribapen osoa

Gorde:
Egile Nagusiak: John Keith Magali, Christine Thomas, Estelle Elisa Ledoux, Yann Capdeville, Sébastien Merkel
Formatua: Artigo
Hizkuntza:Inglês
Argitaratua: Wiley 2025-03-01
Saila:Geochemistry, Geophysics, Geosystems
Gaiak:
transition zone
wadsleyite
olivine
texture
subduction
anisotropy
Sarrera elektronikoa:https://doi.org/10.1029/2024GC011827
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