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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6049884/ https://www.ncbi.nlm.nih.gov/pubmed/30034981 http://dx.doi.org/10.1002/2017JB014394 |