A case study of the amount and distribution of heat and fluid during metamorphism
- 1 March 1980
- journal article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 71 (4) , 373-385
- https://doi.org/10.1007/bf00374708
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- Are thermal domes heated by CO2-rich fluids from the mantle?Published by Elsevier ,2002
- Reaction mechanisms, physical conditions, and mass transfer during hydrothermal alteration of mica and feldspar in granitic rocks from south-central Maine, USAContributions to Mineralogy and Petrology, 1979
- Fluid interaction between granite and sediment during metamorphism, South-central MaineAmerican Journal of Science, 1978
- Transport phenomena in hydrothermal systems; cooling plutonsAmerican Journal of Science, 1977
- Metamorphism of calcareous sediments in the Waterville-Vassalboro area, South-central Maine; mineral reactions and graphical analysisAmerican Journal of Science, 1976
- P, T, $$f_{{\text{CO}}_{\text{2}} }$$ and $$f_{{\text{H}}_{\text{2}} {\text{O}}}$$ during metamorphism of calcareous sediments in the Waterville-Vassalboro area, south-central MaineContributions to Mineralogy and Petrology, 1976
- The Application of Oxygen and Hydrogen Isotope Studies to Problems of Hydrothermal Alteration and Ore DepositionEconomic Geology, 1974
- Correction factors for electron probe microanalysis of silicates, oxides, carbonates, phosphates, and sulfatesAnalytical Chemistry, 1970
- Empirical Correction Factors for the Electron Microanalysis of Silicates and OxidesThe Journal of Geology, 1968
- The Hallowell granite, south central MaineAmerican Journal of Science, 1964