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From the following article:

Spin transition of iron in magnesiowüstite in the Earth's lower mantle

Jung-Fu Lin, Viktor V. Struzhkin, Steven D. Jacobsen, Michael Y. Hu, Paul Chow, Jennifer Kung, Haozhe Liu, Ho-kwang Mao & Russell J. Hemley

Nature 436, 377-380(21 July 2005)

doi:10.1038/nature03825

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Figure 1 - Unfortunately we are unable to provide accessible alternative text for this. If you require assistance to access this image, or to obtain a text description, please contact npg@nature.com

Figure 1

Representative X-ray emission spectra of Fe-Kbeta collected from a single-crystal magnesiowüstite, (Mg0.75,Fe0.25)O, in left fence110right fence orientation at high pressures.

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Figure 2

Normalized volume of magnesiowüstite, (Mg0.83,Fe0.17)O, as a function of pressure at 300 K.

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Figure 3

Calculated isothermal bulk modulus and bulk sound velocity as a function of pressure for the high-spin and low-spin states.

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