The stability of lawsonite and zoisite at high pressures: Experiments in CASH to 92 kbar and implications for the presence of hydrous phases in subducted lithosphere
- 30 June 1994
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 124 (1-4) , 105-118
- https://doi.org/10.1016/0012-821x(94)00080-8
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- An enlarged and updated internally consistent thermodynamic dataset with uncertainties and correlations: the system K2O–Na2O–CaO–MgO–MnO–FeO–Fe2O3–Al2O3–TiO2–SiO2–C–H2–O2Journal of Metamorphic Geology, 1990
- An internally consistent thermodynamic dataset with uncertainties and correlations: 1. Methods and a worked exampleJournal of Metamorphic Geology, 1985
- Relative Stability of Fe-Free Zoisite and ClinozoisiteThe Journal of Geology, 1985
- Calculation of the thermodynamic consequences of dehydration in subducting oceanic crust to 100 kb and > 800 degrees CAmerican Journal of Science, 1978
- Direct determination of coesite- stishovite transition by in-situ X-ray measurementsTectonophysics, 1976
- Equilibria in the system Al 2 O 3 -SiO 2 -H 2 O involving the stability limits of pyrophyllite, and thermodynamic data of pyrophylliteAmerican Journal of Science, 1973
- Determination of Internally Consistent Thermodynamic Data from Phase Equilibrium ExperimentsThe Journal of Geology, 1973
- Experiments on the upper stability limit of pyrophyllite at 1.8 kb and 3.9 kb water pressureAmerican Journal of Science, 1968
- A study of equilibrium relations in the systems Al 2 O 3 -SiO 2 -H 2 O and Al 2 O 3 -H 2 OAmerican Journal of Science, 1967
- Lawsonite equilibriaAmerican Journal of Science, 1965