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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...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2017
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5652234/ https://www.ncbi.nlm.nih.gov/pubmed/29097907 http://dx.doi.org/10.1002/2017GC006850 |