An investigation of disequilibrium growth processes of plagioclase in the system anorthite-albite-water by methods of numerical simulation
- 1 May 1981
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 76 (2) , 196-205
- https://doi.org/10.1007/bf00371959
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Rates and processes of crystal growth in the system anorthite‐albiteJournal of Geophysical Research, 1979
- Multicomponent diffusion in garnet; I, Formulation of isothermal modelsAmerican Journal of Science, 1978
- Melting of plagioclase in the system Ab ? An ? $${\text{H}}_{\text{2}} {\text{O}}$$ and Qz ? Ab ? An ? $${\text{H}}_{\text{2}} {\text{O}}$$ at P H 2 O =5 kbars, an equilibrium problemContributions to Mineralogy and Petrology, 1978
- The importance of adsorption in igneous partitioning of trace elementsGeochimica et Cosmochimica Acta, 1977
- Kinetics of crystal growth from silicate melts: Anorthite and diopsideJournal of Geophysical Research, 1976
- Calculated diffusion coefficients and the growth rate of olivine in a basalt magmaLithos, 1975
- Solute redistribution during crystallization at constant velocity and constant temperatureJournal of Crystal Growth, 1974
- The viscosity of magmatic silicate liquids; a model calculationAmerican Journal of Science, 1972
- Polymer model of silicate meltsGeochimica et Cosmochimica Acta, 1971
- Structural Characteristics of Liquid Mixtures of Feldspar and SilicaJournal of the American Ceramic Society, 1968