Textures Induced by the Coesite‐Stishovite Transition and Implications for the Visibility of the X‐Discontinuity

Textures Induced by the Coesite‐Stishovite Transition and Implications for the Visibility of the X‐Discontinuity

Abstract The coesite‐stishovite phase transition is considered the most plausible candidate to explain the X‐discontinuity observed at around 300 km depth in a variety of tectonic settings. Here, we investigate the microstructure in SiO2 across the coesite‐stishovite transition in uniaxial compressi...

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Bibliographic Details
Main Authors: Matthias Krug, Morvarid Saki, Estelle Ledoux, Jeffrey P. Gay, Julien Chantel, Anna Pakhomova, Rachel Husband, Arno Rohrbach, Stephan Klemme, Christine Thomas, Sébastien Merkel, Carmen Sanchez‐Valle
Format: Article
Language:English
Published: Wiley 2022-10-01
Series:Geochemistry, Geophysics, Geosystems
Subjects:
coesite‐stishovite transition
microstructures
multigrain crystallography
X‐discontinuity
reflection coefficients
mantle heterogeneities
Online Access:https://doi.org/10.1029/2022GC010544

Internet

https://doi.org/10.1029/2022GC010544

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