Genesis and mobility of the H2O-CO2fluid phase during regional greenschist and epidote amphibolite facies metamorphism: a petrological and stable isotope study in the Scottish Dalradian-Reference-Cited by-同舟云学术

Genesis and mobility of the H2O-CO2fluid phase during regional greenschist and epidote amphibolite facies metamorphism: a petrological and stable isotope study in the Scottish Dalradian

Published:1983-07 Issue:4 Volume:140 Page:577-599
ISSN:0016-7649
Container-title:Journal of the Geological Society
language:en
Short-container-title:Journal of the Geological Society

Author:

Graham C. M.,Greig K. M.,Sheppard S. M. F.,Turi B.

Publisher

Geological Society of London

Subject

Geology

Reference47 articles.

1. Slopes, submarine fans, and syndepositional faults: sedimentology of parts of the Middle and Upper Dalradian in the SW Highlands of Scotland;Anderton,1979

2. Mixed volatile equilibria in greenschist facies metabasalts;Best,1978

3. Calcite-dolomite geothermometry for iron-bearing carbonates

4. Burnham C. W. Holloway J. R. Davis N. F. (1969) Thermodynamic properties of water to 1000°C and 10,000 bars. Spec. Pap. geol. Soc. Am 132.

5. Metamorphism in relation to structure in the Scottish Highlands;Elles;Trans. R. Soc. Edinburgh,1930

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