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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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| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2014
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| Matèries: | |
| Accés en línia: | 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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