Fluid Flow during Metamorphism and its Implications for Fluid—Rock Ratios
- 1 January 1986
- book chapter
- Published by Springer Nature
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- A Biotite Isograd in South-Central Maine, U.S.A.: Mineral Reactions, Fluid Transfer, and Heat TransferJournal of Petrology, 1984
- High fluid pressures during regional metamorphism and deformation: Implications for mass transport and deformation mechanismsJournal of Geophysical Research, 1984
- The role of pore water circulation during the deformation of foreland fold and thrust beltsJournal of Geophysical Research, 1984
- The role of the fluid phase during regional metamorphism and deformationJournal of Metamorphic Geology, 1983
- Correction of Holloway's (1977) adaptation of the modified Redlich-Kwong equation of state for calculation of the fugacities of molecular species in supercritical fluids of geologic interestContributions to Mineralogy and Petrology, 1979
- The occurrence of paragonite in chloritoid schists from Stonehaven, ScotlandMineralogical Magazine, 1977
- The sillimanite-potash feldspar isograd in Western Maine, U.S.A.Contributions to Mineralogy and Petrology, 1966
- Almandine in Thermal AureolesJournal of Petrology, 1962
- Pelitic Gneisses with varying Ferrous/Ferric Ratios from Glen Clova, Angus, ScotlandJournal of Petrology, 1960
- CONTACT METAMORPHISM OF MAGNESIAN LIMESTONES AT CRESTMORE, CALIFORNIAGSA Bulletin, 1959