Melting of iron–silicon alloy up to the core–mantle boundary pressure: implications to the thermal structure of the Earth’s core-Reference-Cited by-同舟云学术

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Melting of iron–silicon alloy up to the core–mantle boundary pressure: implications to the thermal structure of the Earth’s core

Published:2009-11-10 Issue:6 Volume:37 Page:353-359
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Asanuma Hidetoshi,Ohtani Eiji,Sakai Takeshi,Terasaki Hidenori,Kamada Seiji,Kondo Tadashi,Kikegawa Takumi

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-009-0338-7.pdf

Reference26 articles.

1. Allègre CJ, Poirier JP, Humler E, Hofmann AW (1995) The chemical composition of the Earth. Earth Planet Sci Lett 134:515–526

2. Balchan AS, Cowan GR (1966) Shock compression of 2 iron–silicon alloys to 2.7 Megabars. J Geophys Res 71:3577–3588

3. Birch F (1952) Elasticity and constitution of the Earth’s interior. J Geophys Res 57:227–286

4. Birch F (1964) Density and composition of mantle and core. J Geophys Res 69:4377–4388

5. Boehler R (1993) Temperatures in the Earth’s core from melting-point measurements of iron at high static pressures. Nature 363:534–536

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