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Constraints on the anisotropic contributions to velocity discontinuities at ∼60 km depth beneath the Pacific
Strong, sharp, negative seismic discontinuities, velocity decreases with depth, are observed beneath the Pacific seafloor at ∼60 km depth. It has been suggested that these are caused by an increase in radial anisotropy with depth, which occurs in global surface wave models. Here we test this hypothe...
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| Publicado no: | Geochem Geophys Geosyst |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
John Wiley and Sons Inc.
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5652234/ https://ncbi.nlm.nih.gov/pubmed/29097907 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2017GC006850 |
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