Solution behavior of +4 cations in high silica melts: petrologic and geochemical implications
- 1 November 1986
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 94 (3) , 343-351
- https://doi.org/10.1007/bf00371443
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Effects of silicate liquid composition on mineral‐liquid element partitioning from Soret diffusion studiesJournal of Geophysical Research, 1986
- Rutile solubility and titanium coordination in silicate meltsGeochimica et Cosmochimica Acta, 1985
- Bishop Tuff Revisited: New Rare Earth Element Data Consistent with Crystal FractionationScience, 1984
- Thermochemical study of glasses in the system NaAlSi3O8-KAlSi3O8-Si4O8 and the join Na1.6Al1.6Si2.4O8-K1.6Al1.6Si2.4O8Geochimica et Cosmochimica Acta, 1984
- Kinetics of zircon dissolution and zirconium diffusion in granitic melts of variable water contentContributions to Mineralogy and Petrology, 1983
- Chemical differentiation of the Bishop Tuff and other high-silica magmas through crystallization processesGeology, 1983
- Large partition coefficients for trace elements in high-silica rhyolitesGeochimica et Cosmochimica Acta, 1983
- Depletion of light rare-earth elements in felsic magmasGeology, 1982
- Pleistocene high‐silica rhyolites of the Coso Volcanic Field, Inyo County, CaliforniaJournal of Geophysical Research, 1981
- Chemical evolution of a pleistocene rhyolitic center: Sierra La Primavera, Jalisco, M xicoContributions to Mineralogy and Petrology, 1981