Carregant...
The origin of secondary microseism Love waves
The interaction of ocean surface waves produces pressure fluctuations at the seafloor capable of generating seismic waves in the solid Earth. The accepted mechanism satisfactorily explains secondary microseisms of the Rayleigh type, but it does not justify the presence of transversely polarized Love...
Guardat en:
| Publicat a: | Proc Natl Acad Sci U S A |
|---|---|
| Autors principals: | , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2020
|
| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7703644/ https://ncbi.nlm.nih.gov/pubmed/33168742 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.2013806117 |
| Etiquetes: |
Afegir etiqueta
Sense etiquetes, Sigues el primer a etiquetar aquest registre!
|