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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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| Publicado en: | J Geophys Res Solid Earth |
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| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
John Wiley and Sons Inc.
2018
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| Assuntos: | |
| 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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