The combined effect of F and H2O on interdiffusion between peralkaline dacitic and rhyolitic melts
- 1 January 1994
- journal article
- research article
- Published by Springer Science and Business Media LLC in Beiträge zur Mineralogie und Petrographie
- Vol. 117 (2), 203-214
- https://doi.org/10.1007/bf00286843
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- Estimation of diffusion coefficients during interdiffusion of geologic melts: Application of transition state theoryChemical Geology, 1992
- Tracer diffusion of network formers and multicomponent diffusion in dacitic and rhyolitic meltsGeochimica et Cosmochimica Acta, 1992
- Interdiffusion of hydrous dacitic and rhyolitic melts and the efficacy of rhyolite contamination of dacitic enclavesBeiträge zur Mineralogie und Petrographie, 1991
- The Nd- and Sr-isotopic composition of I-type microgranitoid enclaves and their host rocks from the Swifts Creek Pluton, southeast AustraliaChemical Geology, 1990
- Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambersBeiträge zur Mineralogie und Petrographie, 1990
- Tracer versus trace element diffusion: Diffusional decoupling of Sr concentration from Sr isotope compositionGeochimica et Cosmochimica Acta, 1989
- Magmatic inclusions in silicic and intermediate volcanic rocksJournal of Geophysical Research, 1986
- Sr and Pb isotopes, U and Th chemistry of the alkaline Monteregian and White Mountain igneous provinces, eastern North AmericaGeochimica et Cosmochimica Acta, 1985
- Crustal influence in the generation of continental flood basaltsNature, 1981
- Water and magmas; a mixing modelGeochimica et Cosmochimica Acta, 1975