Interstitial hydrogen atoms in face-centered cubic iron in the Earth’s core
Author:
Funder
MEXT | Japan Society for the Promotion of Science
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-019-43601-z.pdf
Reference26 articles.
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2. Narygina, O. et al. X-ray diffraction and Mossbauer spectroscopy study of fcc iron hydride FeH at high pressures and implications for the composition of the Earth’s core. Earth Planet. Sci. Lett. 307, 409–414, https://doi.org/10.1016/j.epsl.2011.05.015 (2011).
3. Thompson, E. C. et al. High-Pressure Geophysical Properties of fcc Phase FeHx. Geochem. Geophys. Geosys. 19, 305–314, https://doi.org/10.1002/2017GC007168 (2018).
4. Shibazaki, Y. et al. Sound velocity measurements in dhcp-FeH up to 70 GPa with inelastic X-ray scattering: Implications for the composition of the Earth’s core. Earth Planet. Sci. Lett. 313–314, 79–85, https://doi.org/10.1016/j.epsl.2011.11.002 (2012).
5. Hirao, N. et al. Compression of iron hydride to 80 GPa and hydrogen in the Earth’s inner core. Geophys. Res. Lett. 31, L06616, https://doi.org/10.1029/2003GL019380 (2004).
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