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Constraints on Olivine Deformation From SKS Shear‐Wave Splitting Beneath the Southern Cascadia Subduction Zone Back‐Arc

Abstract Shear‐wave splitting observations of SKS and SKKS phases have been used widely to map azimuthal anisotropy, as caused by the occurrence of olivine, to constrain the dominant directions of upper mantle deformation. While SK(K)S splitting measurements at individual seismic stations are often...

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Bibliografiset tiedot
Päätekijät: E. Löberich, M. D. Long, L. S. Wagner, E. Qorbani, G. Bokelmann
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Wiley 2021-11-01
Sarja:Geochemistry, Geophysics, Geosystems
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Linkit:https://doi.org/10.1029/2021GC010091
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