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Hemispherical anisotropic patterns of the Earth’s inner core

It has been shown that the Earth’s inner core has an axisymmetric anisotropic structure with seismic waves traveling ∼3% faster along polar paths than along equatorial directions. Hemispherical anisotropic patterns of the solid Earth’s core are rather complex, and the commonly used hexagonal-close-p...

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Autors principals: Mattesini, Maurizio, Belonoshko, Anatoly B., Buforn, Elisa, Ramírez, María, Simak, Sergei I., Udías, Agustín, Mao, Ho-Kwang, Ahuja, Rajeev
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2010
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Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC2906852/
https://ncbi.nlm.nih.gov/pubmed/20457937
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1004856107
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