Caricamento...
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...
Salvato in:
| Pubblicato in: | J Geophys Res Solid Earth |
|---|---|
| Autori principali: | , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
John Wiley and Sons Inc.
2018
|
| Soggetti: | |
| Accesso online: | 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 |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne! !
|