Melting of enstatite (MgSiO3) from 10 to 16.5 GPa and the forsterite (Mg2SiO4)-majorite (MgSiO3) eutectic at 16.5 GPa: Implications for the origin of the mantle-Reference-Cited by-同舟云学术

Melting of enstatite (MgSiO3) from 10 to 16.5 GPa and the forsterite (Mg2SiO4)-majorite (MgSiO3) eutectic at 16.5 GPa: Implications for the origin of the mantle

Published:1990 Issue:B10 Volume:95 Page:15771
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Presnall D. C.,Gasparik T.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v095/iB10/JB095iB10p15771/JB095iB10p15771.pdf

Reference43 articles.

1. Solid solubility of Al2O3 in enstatite at high temperatures and 1–5 kb water pressure;Anastasiou;Contrib. Mineral. Petrol.,1972

2. The system anorthite-forsterite-silica;Andersen;Am. J. Sci.,1915

3. Isotopic evolution of the mantle: A model;Anderson;Earth Planet. Sci. Lett.,1982

4. The ternary system diopside-forsterite-silica;Bowen;Am. J. Sci.,1914

5. The binary system MgO-SiO2;Bowen;Am. J. Sci.,1914

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