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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001 1986044982
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005 20190221165132.0
008 190110s1981 xxk 0 0 eng d
040 |a ViAlAGI  |c ViAlAGI 
072 7 |a 05A  |2 georeft 
072 7 |a 02D  |2 georeft 
100 1 |a Graham, Colin M.  |e analytic author 
245 1 0 |a Stable isotope equilibrium and the fluid phase in cooling metamorphic rocks 
300 |a p. 185-186 
500 |a In English 
500 |a Abstract number: 83M/4498 
500 |a Abstractor: C.M.B.H. 
500 |a Key title: Progress in Experimental Petrology 
500 |a Source note: 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 
500 |a Publication type: journal article 
510 3 |a 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 
520 |a If metamorphic assemblages cool in the presence of H<2`O, T's deduced from O isotopes may have no absolute significance unless mineral pairs have similar O diffusion coefficients. 
650 7 |a Activation energy  |2 georeft 
650 7 |a Amphibolite facies  |2 georeft 
650 7 |a Blueschist facies  |2 georeft 
650 7 |a Cooling  |2 georeft 
650 7 |a Experimental studies  |2 georeft 
650 7 |a Facies  |2 georeft 
650 7 |a Fluid phase  |2 georeft 
650 7 |a Isotopes  |2 georeft 
650 7 |a Metamorphic rocks  |2 georeft 
650 7 |a Phase equilibria  |2 georeft 
650 7 |a Stable isotopes  |2 georeft 
773 0 |a Ford, C. E., editor  |t Progress in experimental petrology, Fifth progress report of research supported by N.E.R.C. 1978-1980  |d London : Natural Environment Research Council, 1981  |k Progress in Experimental Petrology  |x 0309-6882  |y PEPEDD  |n 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 type: journal article  |g Vol. 5