Fluid composition and evolution in coesite-bearing rocks (Dora-Maira massif, Western Alps): implications for element recycling during subduction
- 1 August 1995
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 121 (1) , 29-44
- https://doi.org/10.1007/s004100050088
Abstract
No abstract availableKeywords
This publication has 47 references indexed in Scilit:
- Stable isotopic and trace element evidence for restricted fluid migration in 2 GPa eclogitesJournal of Metamorphic Geology, 1994
- Elliptical multilayer Bragg-Fresnel lenses with submicron spatial resolution for X-raysOptics Communications, 1994
- Evidence for low-temperature ultrapotassic siliceous fluids in subduction zone environments from experiments in the system K2OMgOAl2O3SiO2H2O (KMASH)Lithos, 1992
- Short-Lived Radioactivity and Magma GenesisScience, 1992
- Deformation processes in eclogitic rocks: evidence for the rheological delamination of the oceanic crust in deeper levels of subduction zonesJournal of Structural Geology, 1992
- Fluid inclusions in granulites and eclogites from the Bergen Arcs, Caledonides of W. NorwayMineralogical Magazine, 1990
- 40Ar/39Ar laser-probe dating by step heating and spot fusion of phengites from the Dora Maira nappe of the western Alps, ItalyGeology, 1990
- Synthetic fluid inclusions ‐ VII. Re‐equilibration of fluid inclusions in quartz during laboratory‐simulated metamorphic burial and upliftJournal of Metamorphic Geology, 1989
- Coesite in subducted continental crust: P-T history deduced from an elastic modelEarth and Planetary Science Letters, 1984
- Whiteschists: Their compositions and pressure-temperature regimes based on experimental, field, and petrographic evidenceTectonophysics, 1977