Melting temperature distribution and fractionation in the lower mantle-Reference-Cited by-同舟云学术

Melting temperature distribution and fractionation in the lower mantle

Published:1983-08 Issue:1 Volume:33 Page:12-25
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:

Ohtani Eiji

Publisher

Elsevier BV

Subject

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

Reference92 articles.

1. Effect of pressure on the melting of olivine and spinel polymorph of Fe2SiO4;Akimoto;J. Geophys. Res.,1967

2. High pressure crystal chemistry in orthosilicates and formation of the mantle transition zone;Akimoto,1976

3. The high temperature acoustic Grüneisen parameter in the Earth's interior;Anderson;Phys. Earth Planet. Inter.,1979

4. Some elastic constant data relevant to geophysics;Anderson;Rev. Geophys.,1968

5. Iron-magnesium distribution coefficients between spinel [(MgFe)2SiO4], magnesiowüstite [(MgFe)O], and perovskite [(MgFe)SiO3];Bell;Carnegie Inst. Washington Yearb.,1979

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