Petrological characterization of the source components of potassic magmas: geochemical and experimental constraints
- 1 November 1992
- Vol. 28 (3-6) , 187-204
- https://doi.org/10.1016/0024-4937(92)90006-k
Abstract
No abstract availableKeywords
This publication has 59 references indexed in Scilit:
- Phase relations of titan-phlogopite, K2Mg4TiAl2Si6O20(OH)4: a refractory phase in the upper mantle?Published by Elsevier ,2002
- Fluorine-bearing phases in lamproitesTschermaks Mineralogische und Petrographische Mitteilungen, 1991
- The liquidus surface of the system forsterite - kalsilite - quartz at 28 kb under dry conditions, in presence of H2O, and of CO2Tschermaks Mineralogische und Petrographische Mitteilungen, 1988
- The oxidation state of lamproitic magmasTschermaks Mineralogische und Petrographische Mitteilungen, 1985
- Stability of sanidine + forsterite and its bearing on the genesis of potassic magmas and the distribution of potassium in the upper mantleEarth and Planetary Science Letters, 1980
- The origins of potassic magmas; 1, Melting relations in the systems KAlSiO 4 -Mg 2 SiO 4 -SiO 2 and KAlSiO 4 MgO-SiO 2 -CO 2 to 30 kilobarsAmerican Journal of Science, 1980
- Origin of olivine melilitites — chemical and experimental constraintsJournal of Volcanology and Geothermal Research, 1978
- Titanium solubility in synthetic phlogopite solid solutionsChemical Geology, 1976
- XIV.—The Kalsilite-bearing Lavas of Kabirenge and Lyakauli, South-West UgandaTransactions of the Royal Society of Edinburgh, 1947
- A suite of volcanic rocks from south-west Uganda containing kalsilite (a polymorph of KAlSiO4)Mineralogical Magazine and Journal of the Mineralogical Society, 1942