Hydrogarnet substitution in pyrope: a possible location for “water” in the mantle
Authors:
- L. AckermannLAL. Ackermann
- L. CemičLCL. Cemič
- K. LangerKLK. Langer
- 1 February 1983
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 62 (2) , 208-214
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Mechanism of the water and carbon dioxide solubility in oxides and silicates and the role of O?Contributions to Mineralogy and Petrology, 1981
- Messung des Ultrarot-Pleochroismus von Mineralen. XIV. Der Pleochroismus der OH-Streckfrequenz in DiopsidMineralogy and Petrology, 1976
- 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
- Titanoclinohumite: A possible mineralogical site for water in the upper mantleJournal of Geophysical Research, 1970
- Pressure dependence of crystal structures in the system MgOAl2O3SiO2H2O at pressures up to 30 kilobarsPhysics of the Earth and Planetary Interiors, 1970
- Lattice energies, phase transformations and volatiles in the mantlePhysics of the Earth and Planetary Interiors, 1970
- Mica in the upper mantleContributions to Mineralogy and Petrology, 1969
- The genesis of basaltic magmasContributions to Mineralogy and Petrology, 1967
- Stability of phlogopite at high pressures and possible presence of phlogopite in the earth's upper mantleEarth and Planetary Science Letters, 1967
- Petrological Evidence for the Presence of Amphibole in the Upper Mantle and its Petrogenetic and Geophysical ImplicationsGeological Magazine, 1964