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Seismological expression of the iron spin crossover in ferropericlase in the Earth’s lower mantle
The two most abundant minerals in the Earth’s lower mantle are bridgmanite and ferropericlase. The bulk modulus of ferropericlase (Fp) softens as iron d-electrons transition from a high-spin to low-spin state, affecting the seismic compressional velocity but not the shear velocity. Here, we identify...
Autores principales: | Shephard, Grace E., Houser, Christine, Hernlund, John W., Valencia-Cardona, Juan J., Trønnes, Reidar G., Wentzcovitch, Renata M. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8501025/ https://www.ncbi.nlm.nih.gov/pubmed/34625555 http://dx.doi.org/10.1038/s41467-021-26115-z |
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