Phase relations of titan-phlogopite, K2Mg4TiAl2Si6O20(OH)4: a refractory phase in the upper mantle?
- 1 April 1974
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 22 (1), 60-66
- https://doi.org/10.1016/0012-821x(74)90064-8
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- 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
- Contrasted melting relations in a pyrolite upper mantle under mid-oceanic ridge, stable crust and island arc environmentsTectonophysics, 1973
- Origin of some magmas in oceanic and circum-oceanic regionsTectonophysics, 1973
- Volcanism and orogenic belts — The origin of andesitesTectonophysics, 1973
- Conditions of melting of basanite magma from garnet peridotiteEarth and Planetary Science Letters, 1973
- The stability of phlogopite + enstatite at high pressures; a model for micas in the interior of the EarthAmerican Journal of Science, 1972
- Magmatic activity as the major process in the chemical evolution of the earth's crust and mantleTectonophysics, 1972
- V. Petrogenesis and discussionPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971
- Variations of Major Chemical Constituents across the Central Sierra Nevada BatholithGSA Bulletin, 1970
- Phlogopite from Jan Mayen Island (North Atlantic)Earth and Planetary Science Letters, 1969