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...
| المؤلفون الرئيسيون: | , , , , , |
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| التنسيق: | Journal article |
| اللغة: | English |
| منشور في: |
2005
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