Post‐perovskite phase transition and mineral chemistry in the pyrolitic lowermost mantle

By M. Murakami, K. Hirose, N. Sata, Y. Ohishi. 2005

213 citations recorded by the source corpus.

Subfields: Geophysics

View Paper: https://www.semanticscholar.org/paper/e0897f4339f9ef5c568ada93d7edf976a799f43e

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In Geophysics

1. K. Hirose
2. J. Hernlund
3. C. Houser

Citations in the corpus

• Very low sound velocities in iron‐rich (Mg,Fe)O: Implications for the core‐mantle boundary region (2010, background): “Additionally, recent experimental results, based on analyses of quenched phase assemblages from P ∼ 100 GPa and T ∼1800 K, suggest that iron preferentially partitions into (Mg,Fe)O in the presence of Pv‐ and PPv‐structured silicates [ Murakami et al., 2005; Auzende et al., 2008; Sinmyo et al., 2008”
• Postperovskite phase transition and its geophysical implications (2006, background): “…in both synthetic and natural systems: (Mg,Fe)SiO3 [Mao et al., 2004; Shieh et al., 2006], (Mg,Fe)2SiO4 [Hirose et al., 2006a], Mg3Al2Si3O12 [Tateno et al., 2005], natural pyrolite (KLB-1 peridotite) [Murakami et al., 2005; Ono and Oganov, 2005], and MORB compositions [Hirose et al., 2005a].”