The olivine-spinel transition in Fe2SiO4and Ni2SiO4-Reference-Cited by-同舟云学术

The olivine-spinel transition in Fe2SiO4and Ni2SiO4

Published:1965-04-15 Issue:8 Volume:70 Page:1969-1977
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Akimoto Syun-iti,Fujisawa Hideyuki,Katsura Takashi

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/jz/v070/i008/JZ070i008p01969/JZ070i008p01969.pdf

Reference23 articles.

1. Demonstration of the electrical conductivity jump produced by the olivine-spinel transition;Akimoto;J. Geophys. Res.,1965

2. Synthesis of FeSiO3 pyroxene (ferrosilite) at high pressures;Akimoto;Proc. Japan Acad.,1964

3. Elasticity and constitution of the earth's interior;Birch;J. Geophys. Res.,1952

4. The fayalite-Fe2SiO4 spinel transition;Boyd;Carnegie Inst. Wash. Year Book,1960

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