Stable isotope equilibrium and the fluid phase in cooling metamorphic rocks

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Authors:Graham, Colin M.
Volume Title:Progress in experimental petrology, Fifth progress report of research supported by N.E.R.C. 1978-1980
Volume Authors:Ford, C. E., editor
Source:Progress in experimental petrology, Fifth progress report of research supported by N.E.R.C. 1978-1980, edited by C. E. Ford. Progress in Experimental Petrology, Vol.5, p.185-186. Publisher: Natural Environment Research Council, London, United Kingdom. ISSN: 0309-6882
Publication Date:1981
Note:In English
Summary:If metamorphic assemblages cool in the presence of H2O, T's deduced from O isotopes may have no absolute significance unless mineral pairs have similar O diffusion coefficients. [C.M.B.H.]
Subjects:Activation energy; Amphibolite facies; Blueschist facies; Cooling; Experimental studies; Facies; Fluid phase; Isotopes; Metamorphic rocks; Phase equilibria; Stable isotopes
Abstract Numbers:83M/4498
Record ID:1986044982
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom, Reference includes data from PASCAL, Institute de l'Information Scientifique et Technique
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