Melting relations in the iron-sulfur system at ultra-high pressures: Implications for the thermal state of the Earth

Author:

Williams Quentin,Jeanloz Raymond

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

Reference93 articles.

1. Equations of state of iron sulfide and constraints on the sulfur content of the Earth;Ahrens;J. Geophys. Res.,1979

2. Constraints on core composition from shock-wave data;Ahrens;Philos. Trans. R. Soc. London, Ser. A,1982

3. Pyrite: Shock compression, isentropic release, and composition of the Earth's core;Ahrens;J. Geophys. Res.,1987

4. The Mg2SiO4 polymorphs (olivine, modified spinel and spinel)-thermodynamic properties from oxide melt solution calometry, phase relations, and models of lattice vibrations;Akaogi;Am. Mineral.,1984

5. Mineralogic distribution of iron in the upper half of the transition zone in the Earth's mantle;Akimoto,1976

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