Thermodynamics of the system Fe–Si–O under high pressure and temperature and its implications for Earth’s core
Author:
Funder
H2020 European Research Council
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,General Materials Science
Link
http://link.springer.com/content/pdf/10.1007/s00269-020-01102-w.pdf
Reference50 articles.
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3. Anderson OL, Oda H, Isaak DG (1992) A model for the computation of thermal expansivity at high compression and high temperatures: MgO as an example. Geophys Res Lett 19:1987–1990
4. Antonangeli D, Siebert J, Badro J, Farber DL, Fiquet G, Morard G, Ryerson FJ (2010) Composition of the Earth’s inner core from high-pressure sound velocity measurements in Fe–Ni–Si alloys. Earth Planet Sci Lett 295:292–296
5. Antonangeli D, Morard G, Paolasini L, Garbarino G, Murphy CA, Edmund E, Decremps F, Fiquet G, Bosak A, Mezouar M, Fei YW (2018) Sound velocities and density measurements of solid hcp-Fe and hcp-Fe-Si (9 wt%) alloy at high pressure: constraints on the Si abundance in the Earth’s inner core. Earth Planet Sci Lett 482:446–453
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