The high-pressure stability of hydrous phases in orogenic belts: an experimental approach on eclogite-forming processes
- 1 May 1997
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 273 (1-2) , 169-184
- https://doi.org/10.1016/s0040-1951(96)00293-4
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Oxygen and carbon isotope evidence for seawater-hydrothermal alteration of the Macquarie Island ophiolitePublished by Elsevier ,2002
- H2O transport and release in subduction zones: Experimental constraints on basaltic and andesitic systemsJournal of Geophysical Research, 1995
- Paragonite eclogites from Dabie Shan, China: re‐equilibration during exhumation?Journal of Metamorphic Geology, 1995
- Water Sources for Subduction Zone Volcanism: New Experimental ConstraintsScience, 1993
- The upper thermal stability of chlorite + quartz: an experimental study in the system MgO-Al2O3-SiO2-H2OJournal of Metamorphic Geology, 1989
- An algorithm and computer program for calculating composition phase diagramsCalphad, 1987
- Formation of the volcanic front in subduction zonesGeophysical Research Letters, 1986
- Fluid-absent metamorphismJournal of the Geological Society, 1983
- Regional high-pressure metamorphism in new caledonia: Phase equilibria in the ouégoa districtTectonophysics, 1977
- Rock-water systems, with special reference to the water-deficient regionAmerican Journal of Science, 1971