Steep oxygen-isotope gradients at marble—metagranite contacts in the northwest Adirondack Mountains, New York, USA: products of fluid-hosted diffusion
- 1 October 1991
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 107 (1) , 148-163
- https://doi.org/10.1016/0012-821x(91)90051-i
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- Constraints on effective diffusivity during oxygen isotope exchange at a marble-schist contact, Sifnos (Cyclades), GreecePublished by Elsevier ,2002
- Advective-diffusive transport of isotopic fronts: An example from Naxos, GreeceEarth and Planetary Science Letters, 1990
- Geochemical evidence for a revised Precambrian sequence in the northwest Adirondacks, New YorkGSA Bulletin, 1990
- Isotopic and petrological evidence for the infiltration of water-rich fluids during the Miocene M2 metamorphism on Naxos, GreeceGeochimica et Cosmochimica Acta, 1989
- Advective fluid transport during charnockite formation; an example from southern IndiaEarth and Planetary Science Letters, 1989
- Transport of stable isotopes: I: Development of a kinetic continuum theory for stable isotope transportContributions to Mineralogy and Petrology, 1988
- The transport of heat and matter by fluids during metamorphismContributions to Mineralogy and Petrology, 1987
- Metamorphism in the Adirondacks. I. Petrology, Pressure and TemperatureJournal of Petrology, 1985
- Fluid heterogeneity during granulite facies metamorphism in the Adirondacks: stable isotope evidenceContributions to Mineralogy and Petrology, 1984
- Calc-silicate reactions in Adirondack marbles: The role of fluids and solid solutions: SummaryGSA Bulletin, 1980