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Iron spin transition in Earth's mantle

High-pressure Mössbauer spectroscopy on several compositions across the (Mg,Fe)O magnesiowüstite solid solution confirms that ferrous iron (Fe(2+)) undergoes a high-spin to low-spin transition at pressures and for compositions relevant to the bulk of the Earth's mantle. High-resolution x-ray di...

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Autors principals: Speziale, S., Milner, A., Lee, V. E., Clark, S. M., Pasternak, M. P., Jeanloz, R.
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2005
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Accés en línia:https://ncbi.nlm.nih.gov/pmc/articles/PMC1312404/
https://ncbi.nlm.nih.gov/pubmed/16330758
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0508919102
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