Magnesium grain boundary diffusion in forsterite aggregates at 1000°-1300°C and 0.1 MPa to 10 GPa

Author:

Farver John R.,Yund Richard A.,Rubie David C.

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

Reference43 articles.

1. Self-diffusion in Mg2SiO4 (forsterite) at high temperature;Andersson;Fresenius Z. Anal. Chem.,1989

2. Substantial hydrogen solubility in olivine and implications for water storage in the mantle;Bai;Nature,1992

3. Fe-Mg interdiffusion in olivine from 0.5 to 9 GPa and from 600° to 900°C;Bertran-Alvarez;Eos Trans. AGU,1993

4. Intergranular diffusion in metamorphic rocks;Brady;Am. J. Sci.,1983

5. Mg tracer diffusion in forsterite and San Carlos olivine;Chakraborty;Eos Trans. AGU,1992

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