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...

全面介绍

书目详细资料
Main Authors: Speziale, S, Milner, A, Lee, V, Clark, S, Pasternak, M, Jeanloz, R
格式: Journal article
语言:English
出版: 2005

相似书籍