The MgSiO3system at high pressure: Thermodynamic properties of perovskite, postperovskite, and melt from global inversion of shock and static compression data

Author:

Mosenfelder Jed L.1,Asimow Paul D.1,Frost Daniel J.2,Rubie David C.2,Ahrens Thomas J.13

Affiliation:

1. Division of Geological and Planetary Sciences; California Institute of Technology; Pasadena California USA

2. Bayerisches Geoinstitut; Universität Bayreuth; Bayreuth Germany

3. Lindhurst Laboratory of Experimental Geophysics, Seismological Laboratory; California Institute of Technology; Pasadena California USA

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

Reference79 articles.

1. Static compression and olivine flotation in ultrabasic silicate liquid;Agee;J. Geophys. Res.,1988

2. Heat capacity of MgSiO3 perovskite;Akaogi;Geophys. Res. Lett.,1993

3. Calorimetric study on majorite-perovskite transition in the system Mg4Si4O12-Mg3Al2Si3O12: Transition boundaries with positive pressure-temperature slopes;Akaogi;Phys. Earth Planet. Inter.,1999

4. Akins , J. A. 2003 Dynamic compression of minerals in the MgO-FeO-SiO 2 system Calif. Inst. of Technol. Pasadena, Calif.

5. Shock-induced melting of MgSiO3 perovskite and implications for melts in Earth's lowermost mantle;Akins;Geophys. Res. Lett.,2004

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