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Apparent Splitting of S Waves Propagating Through an Isotropic Lowermost Mantle

Observations of shear wave anisotropy are key for understanding the mineralogical structure and flow in the mantle. Several researchers have reported the presence of seismic anisotropy in the lowermost 150–250 km of the mantle (i.e., D [Formula: see text] layer), based on differences in the arrival...

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Detalles Bibliográficos
Publicado en:J Geophys Res Solid Earth
Main Authors: Parisi, Laura, Ferreira, Ana M. G., Ritsema, Jeroen
Formato: Artigo
Idioma:Inglês
Publicado: John Wiley and Sons Inc. 2018
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Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC6049884/
https://ncbi.nlm.nih.gov/pubmed/30034981
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017JB014394
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