Magnesium grain boundary diffusion in forsterite aggregates at 1000°–1300°C and 0.1 MPa to 10 GPa
- 10 October 1994
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 99 (B10) , 19809-19819
- https://doi.org/10.1029/94jb01250
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Substantial hydrogen solubility in olivine and implications for water storage in the mantleNature, 1992
- Numerical evaluation method for the determination of grain-boundary diffusion coefficients from tracer concentration profiles for a constant boundary concentrationPhilosophical Magazine A, 1990
- Grain growth kinetics in olivine aggregatesTectonophysics, 1989
- Critical Appraisal of Diffusivity Determinations from Experimental Creep DataJournal of the American Ceramic Society, 1988
- The catalysis of mineral reactions by water and restrictions on the presence of aqueous fluid during metamorphismMineralogical Magazine, 1986
- On the structure of grain boundaries in tectonitesTectonophysics, 1981
- Oxygen self-diffusion in forsterite: Implications for the high-temperature creep mechanismEarth and Planetary Science Letters, 1980
- The analysis of grain boundary diffusion measurementsBritish Journal of Applied Physics, 1963
- Influence of dislocations on diffusion kinetics in solids with particular reference to the alkali halidesTransactions of the Faraday Society, 1961
- Measurement of Intergranular Diffusion in a Silicate System: Iron in ForsteriteNature, 1959