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Sound Velocities and Equation of State of Iron-Rich (Mg,Fe)O

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Figure

Figure 1.1: Modal mineralogy of the earth’s mantle, assuming a pyrolite mantle. The upper man-tle (0-440 km below the earth’s surface) is mostly comprised of olivine garnet, and pyroxenesand (Mg,Fe)- silicate perovskite and (Mg,Fe)O
Figure 2.4: Raw NRIXS spectra of (Mg.16Fe.84)O at 300 K at different pressures over 0 to 120 GPa,measured at Sector 3-ID-B of the Advanced Photon Source
Figure 2.5: Partial projected phonon density of states (PDOSs) of (Mg.16Fe.84)O, extracted fromthe NRIXS scans using the PHOENIX software.
Figure 2.6: Time spectra of (Mg.16Fe.84)O from synchrotron M¨ossbauer spectroscopy. The ambientpressure spectrum is characterized by slow oscillations, consistent with no magnetic ordering
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