Iron spin transition in Earth's mantle.

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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Bibliografiske detaljer
Main Authors:	Speziale, S, Milner, A, Lee, V, Clark, S, Pasternak, M, Jeanloz, R
Format:	Journal article
Sprog:	English
Udgivet:	2005

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