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Spin crossover in ferropericlase and velocity heterogeneities in the lower mantle

Deciphering the origin of seismic velocity heterogeneities in the mantle is crucial to understanding internal structures and processes at work in the Earth. The spin crossover in iron in ferropericlase (Fp), the second most abundant phase in the lower mantle, introduces unfamiliar effects on seismic...

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Detalles Bibliográficos
Main Authors: Wu, Zhongqing, Wentzcovitch, Renata M.
Formato: Artigo
Idioma:Inglês
Publicado: National Academy of Sciences 2014
Assuntos:
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC4115492/
https://ncbi.nlm.nih.gov/pubmed/25002507
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1322427111
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