Partial melting in the iron–sulfur system at high pressure: A synchrotron X-ray diffraction study-Reference-Cited by-同舟云学术

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Partial melting in the iron–sulfur system at high pressure: A synchrotron X-ray diffraction study

Published:2007-06 Issue:1-2 Volume:162 Page:119-128
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Campbell Andrew J.,Seagle Christopher T.,Heinz Dion L.,Shen Guoyin,Prakapenka Vitali B.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference39 articles.

1. Composition and temperature of Earth's core constrained by combining ab initio calculations and seismic data;Alfè;Earth Planet. Sci. Lett.,2002

2. Abundances of the elements: meteoritic and solar;Anders;Geochim. Cosmochim. Acta,1989

3. Experimental melting curve of iron revisited;Anderson;J. Geophys. Res.,1997

4. Study of partial melting at high pressure using in situ X-ray diffraction;Andrault;High Pres. Res.,2007

5. Model calculations of the temperature distribution in the laser-heated diamond anvil cell;Bodea;J. Appl. Phys.,1989

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