Phase relationships in the system KAlSiO4-Mg2SiO4-SiO2-H2O as a model for hybridization between hydrous siliceous melts and peridotite
- 1 January 1982
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 79 (4) , 368-374
- https://doi.org/10.1007/bf01132066
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- The origins of potassic magmas; 2, Stability of phlogopite in natural spinel lherzolite and in the system KAlSiO 4 -MgO-SiO 2 -H 2 O-CO 2 at high pressures and high temperaturesAmerican Journal of Science, 1980
- Melting Reactions in the System NaAlSi3O8-KAlSi3O8-SiO2 to 35 Kilobars, Dry and with Excess WaterThe Journal of Geology, 1975
- Phase relationships of phlogopite in the system K 2 O-MgO-CaO-Al 2 O 3 -SiO 2 -H 2 O to 35 kilobars; a better model for micas in the interior of the EarthAmerican Journal of Science, 1973
- Effect of Water on Olivine Stability in Tholeiites and the Production of Silica-Saturated Magmas in the Island-Arc EnvironmentThe Journal of Geology, 1973
- The stability of phlogopite + enstatite at high pressures; a model for micas in the interior of the EarthAmerican Journal of Science, 1972
- The System Forsterite Diopside-Silica With and Without Water at High PressuresAmerican Journal of Science, 1969
- Effect of Water on the Melting of EnstatiteGSA Bulletin, 1968
- Studies in the System KAlSiO4--Mg2SiO4--SiO2--H2O: I, Inferred Phase Relations and Petrologic ApplicationsJournal of Petrology, 1967
- The upper three-phase region in the system SiO 2 -H 2 OAmerican Journal of Science, 1962