Constraints on effective diffusivity during oxygen isotope exchange at a marble-schist contact, Sifnos (Cyclades), Greece
- 1 September 1989
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 94 (3-4), 208-216
- https://doi.org/10.1016/0012-821x(89)90140-4
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Isotopic and petrological evidence for the infiltration of water-rich fluids during the Miocene M2 metamorphism on Naxos, GreeceGeochimica et Cosmochimica Acta, 1989
- High integrated fluid/rock ratios during metamorphism at Naxos: evidence from carbon isotopes of calcite in schists and fluid inclusionsContributions to Mineralogy and Petrology, 1988
- Transformation of blueschist to greenschist facies rocks as a consequence of fluid infiltration, Sifnos (Cyclades), GreeceContributions to Mineralogy and Petrology, 1987
- The transport of heat and matter by fluids during metamorphismContributions to Mineralogy and Petrology, 1987
- Fluid evolution and transport during metamorphism: evidence from the Llano Uplift, TexasContributions to Mineralogy and Petrology, 1986
- Stable isotopic evidence for large-scale seawater infiltration in a regional metamorphic terrane; the Trois Seigneurs Massif, Pyrenees, FranceContributions to Mineralogy and Petrology, 1985
- Evolution of the blueschist and greenschist facies rocks of Sifnos, Cyclades, GreeceContributions to Mineralogy and Petrology, 1984
- CO 2 rich fluids during regional metamorphism on Naxos (Greece); carbon isotopes and fluid inclusionsAmerican Journal of Science, 1980
- Are thermal domes heated by CO2-rich fluids from the mantle?Earth and Planetary Science Letters, 1979
- Water/rock interactions and the origin of H 2 O in granitic batholithsJournal of the Geological Society, 1977