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Science, ISSN 0036-8075, 5/2003, Volume 300, Issue 5620, pp. 789 - 791
... kilometers in Earth's lower mantle. This transition implies that the partition coefficient of iron between ferropericlase and magnesium silicate perovskite, the two main constituents of the lower mantle, may increase by several orders... 
Lower mantle | Transition pressure | Artificial satellites | Emission spectra | Reports | Perovskites | Magnetic dipole moment | Iron | Magnesium | Silicates | High pressure | TRANSITION | MAGNESIOWUSTITE | HIGH-PRESSURE | SPECTROSCOPY | SPIN | TEMPERATURE | MULTIDISCIPLINARY SCIENCES | X-RAY-EMISSION | DYNAMICS | (MG,FE)SIO3-PEROVSKITE | SILICATE PEROVSKITE | Earth | Stratification (Geology) | Geology, Structural | Research | Mantle
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Proceedings of the National Academy of Sciences of the United States of America, ISSN 0027-8424, 12/2005, Volume 102, Issue 50, pp. 17918 - 17922
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Journal of Geophysical Research - Solid Earth, ISSN 0148-0227, 04/2002, Volume 107, Issue B4, pp. 2078 - ECV 3-13
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Geophysical Journal International, ISSN 0956-540X, 03/2011, Volume 184, Issue 3, pp. 1180 - 1213
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Journal of the Geological Society, ISSN 0016-7649, 07/2011, Volume 168, Issue 4, pp. 873 - 886
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Journal of Geophysical Research - Solid Earth, ISSN 0148-0227, 05/2008, Volume 113, Issue B5, pp. B05403 - n/a
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