A synchrotron Mössbauer spectroscopy study of (Mg,Fe)SiO3 perovskite up to 120 GPa

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The spin state of iron in minerals of Earth's lower mantle (2005, methodology): “1 could not detect a change in the spin state of Fe(II) up to 120 GPa, however, indications for a changing spin state of Fe(III) around 70 GPa were reported [Jackson et al., 2005].”
Spin state of ferric iron in MgSiO3 perovskite and its effect on elastic properties (2010, background): “, 2008), Fe/ΣFewas notmeasured in those samples, and Mössbauer studies have shown a wide range of Fe/ΣFe values even in the absence of Al (McCammon, 1997; Jackson et al., 2005).”
Solids, liquids, and gases under high pressure (2018, background): “For example, Jackson et al. (2005) measured two silicate perovskite samples Fe0.”
Postperovskite phase transition and its geophysical implications (2006, background): “The spin transition of iron in (Mg,Fe)SiO3 perovskite has been also observed experimentally [Badro et al., 2004; Li et al., 2004; Jackson et al., 2005].”
Valence state and spin transitions of iron in Earth's mantle silicates (2006, methodology): “[11]) if room-temperature compression is performed.”