P Wave Anisotropy Caused by Partial Eclogitization of Descending Crust Demonstrated by Modeling Effective Petrophysical Properties

Abstract Seismological studies of large‐scale processes at convergent plate boundaries typically probe lower crustal structures with wavelengths of several kilometers, whereas field‐based studies typically sample the resulting structures at a much smaller scale. To bridge this gap between scales, we...

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Bibliographic Details
Main Authors: Sascha Zertani, Johannes C. Vrijmoed, Frederik Tilmann, Timm John, Torgeir B. Andersen, Loic Labrousse
Format: Article
Language:English
Published: Wiley 2020-06-01
Series:Geochemistry, Geophysics, Geosystems
Online Access:https://doi.org/10.1029/2019GC008906