Trace element zoning in garnet from the Kwoiek Area, British Columbia: disequilibrium partitioning during garnet growth?
Authors:
- 1 November 1990
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 104 (6) , 619-630
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Rates of Tectonometamorphic Processes from Rubidium and Strontium Isotopes in GarnetScience, 1989
- Lithium in staurolite and its petrologic significanceContributions to Mineralogy and Petrology, 1986
- Metamorphism in the Adirondacks. I. Petrology, Pressure and TemperatureJournal of Petrology, 1985
- Self-diffusion of magnesium in garnet at 750 degrees to 900 degrees CAmerican Journal of Science, 1985
- Crystal growth and the formation of chemical zoning in garnetsContributions to Mineralogy and Petrology, 1982
- Characterization of Grain‐Boundary Segregation in MgOJournal of the American Ceramic Society, 1981
- Partition of trace elements in co-existing biotite, muscovite and potassium feldspar of granitic rocks, northern PortugalChemical Geology, 1975
- Kinetic disequilibrium in trace element partitioning between phenocrysts and host lavaGeochimica et Cosmochimica Acta, 1972
- Phase Equilibria in Three Assemblages of Kyanite-Zone Pelitic Schists, Lincoln Mountain Quadrangle, Central VermontJournal of Petrology, 1965
- The Role of Adsorption in the Fractionation and Distribution of ElementsThe Journal of Geology, 1955