A numerical study of mineral zoning formed during the cooling of finite volume grains
Open Access
- 10 October 1985
- journal article
- regular section
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 90 (B12) , 10351-10358
- https://doi.org/10.1029/jb090ib12p10351
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- Self-diffusion of magnesium in garnet at 750 degrees to 900 degrees CAmerican Journal of Science, 1985
- A geothermobarometric investigation of garnet peridotites in the Western Gneiss Region of NorwayContributions to Mineralogy and Petrology, 1984
- Evaluation of olivine-spinel geothermometry as an indicator of thermal history for peridotitesContributions to Mineralogy and Petrology, 1983
- The Geology of the Great 'Dyke', Zimbabwe: The Ultramafic RocksJournal of Petrology, 1982
- Solute partitioning under continuous cooling conditions as a cooling rate indicatorJournal of Geophysical Research, 1981
- Diffusion in silicate minerals and glasses: A data digest and guide to the literatureContributions to Mineralogy and Petrology, 1981
- Garnet peridotite from Colorado Plateau ultramafic diatremes: Hydrates, carbonates, and comparative geothermometryContributions to Mineralogy and Petrology, 1981
- An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometerContributions to Mineralogy and Petrology, 1979
- The Mathematics of Cation Diffusion and Exchange Between Silicate Minerals During Retrograde MetamorphismPublished by Springer Nature ,1977
- The general linear inverse problem: Implication of surface waves and free oscillations for Earth structureReviews of Geophysics, 1972