Temperature and discontinuities in the transition layer within the Earth's mantle: Geophysical application of the olivine-spinel transition in the Mg2SiO4-Fe2SiO4System-Reference-Cited by-同舟云学术

Temperature and discontinuities in the transition layer within the Earth's mantle: Geophysical application of the olivine-spinel transition in the Mg2SiO4-Fe2SiO4System

Published:1968-05-15 Issue:10 Volume:73 Page:3281-3294
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Fujisawa Hideyuki

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/v073/i010/JB073i010p03281/JB073i010p03281.pdf

Reference50 articles.

1. Olivine-spinel solid solution equilibria in the system Mg2SiO4-Fe2SiO4;Akimoto;Tech. Rept. Inst. Solid State Phys., Univ. of Tokyo, Ser. A,1967

2. High-pressure synthesis of Mg2SiO4 spinel;Akimoto;Earth Planetary Sci. Letters,1966

3. Equation of state for aluminum, copper, and lead in high-pressure region;Al'tshuler;J. Exp. Theoret. Phys. SSSR,1960

4. Shock compression of periclase and quartz and the composition of the lower mantle;Al'tshuler;Izv. Akad. Nauk SSSR, Phys. Solid Earth,1965

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